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THE
ENCYCLOPAEDIA BRITANNICA
DICTIOx\ARY
Arts, Sciences, and General Literature
THE E. S. PEALE EEPEI^-T
WITH NKW MAPS AiNI) ORIGINAL AMERICAN ARTICLES BY EMimm'
WRITERS
VOLUME XVI
their "Enhius."' V. CHICAGO Oriffini
minor poems or_<'v.^ ^ g^ PEA:^ ^"'> ' '''^ \NY ^ ^''''^'
r
HTi&S 708S79
^'
7/
Encyclopaedia '^ Britannica.
Vol. XVI. — (MEN-MOS).
Total number of Articles, 376.
PRINCIPAL CONTENTS.
MENANDER. F. i Palet, LL.D.
\U-NCHJS. jAMr.3 1.EOQE, LL.D., Professor of Cbinese,
UDiversity of Oxfori
MENDELSSOHN. V/. S. Rook«tro, Author of " Life
of HandeL"
MENSURATION. Wm. Thomson, Professor of Mathe-
matics, Stollenbosch College, South Africa.
MERCUEY. W. DiTTMAK, F.R.S., Professor of
Chemistry, Anderson's College, Glas.'jow.
THBRAPEniic Uses. D. J. Leech, 11. D., Profossoi
of Materia Medica, Owens College, Manchester.
MERV. Major F. 0. H. Clarke, C.M.G., R.A.
MESOPOTAMIA. Prof. AiBREonT SooiN. University
of Tubingen.
MES3IAH. Prof. W. RonKRTsoN Smith, LL.D.
METALLURGY. Prof. Dittmar.
METAL-WORK. J. H. Middleton, M.A., London.
METAPHYSIC. Edward Caird, LL.D., Professor of
Moral Philosophy, University of Glasgow.
METASTASIO. J. A. Symokds, M.A.
METEMPSYCHOSIS. F. A. Paiet, LL.D.
METEOR. Hubert A. Newton, LL.D., Professor of
Mathematics, Yale College, Conn.
METEOROLOGY. A. Bhohan, F.R.S.E., and Prof.
Balfodr Stewart, LL.D., F.R.S.
METHODISM. Rev. J. H. Rioo, D.D., Author of
" Chnrchmaffship of John Wesley."
METSU. J. A. Crowe, Author of "Lives of Early
'Flemish Painters."
METTERNICH. C. Alan Ftffe, M.A., Author of
"A History of Modern Europe."
MEXICO. E. B. Tyloe, D.C.L., LL.D., F.R.S., and
Prof. A. H. Eeane.
MEYERBEER. W. S. RocKSTRO.
MICAH. Prof. W. Robertson Smith.
MICHELANGELO. Sidney Colvik, M.A., SladePro
fessor of Fine Art, University of Cambridge.
MICH IGAN. 0. K. Adams, LL. D., Professor ef History,
University of Michigan, Ann Arbor, Mich.
MICROMETER. David Gill, LL.D., F.R.S., Astro-
nomer-Royal, Cape of Good Hope.
MICROSCOPE. W. B. Carpenter, M.D., C.B.,
F.R.S., A'lthor of "The Microscope and its Revela-
tions."
MIDDLESEX. H. B. Wheatley, Secretary of the
Topographical Society of London.
MIDKASH. S. M. SohilleeSzinessy, M.A,
MILITARY LAW. J. C. 0'Do^\-D, C.B., D-put}
Judge Advocate General, War Office, Loudon.
MILITIA. J. C. O'DowD.
MILK. Prof. J. G. M'Kendriok, M.D., LL.D., and
James Paton.
MILL, JAMES. Alexander Bain, LL.D., Author of
"The Emotions and the Will."
MILL, JOHN STUART. Wm. Minto, M.A., Professoi
of LoKic, University of Aberdeen.
MILLENNIUM. Adolf Harnack, D.D., Professor
of Church History, University of Giessen.
MILLER, HUGH: Peteii Bayne, LL.D.. Author of
" Life and Letters of Hugh Miller."
MILMAN. Richard Gaknett, LL.D.
MILTON. Prof. David Masson, LL.D., Author 0
" Life of John Milton."
MILWAUKEE. J. Jouhstok, Milwaukee.
MIMICRY. Grant Ai.i.en.
MINERALOGY. M. F. Heddle, M.D., Professor of
Chemistry, University of St Andrews.
MINERAL WATERS. John Macpheeson, M.D.,
Author of " Baths and Wells of Europe," and Prof.
Albert R. Leeds, Stovens Institute of Technology,
Hoboken, N.J.
MINIATURE. E. Mafnde Thompson, LL.D.
MINING. C. Le Neve Foster, D.Sc, H.M. In-
spector of Metalliferous Mines.
MINISTRY. Alex. C. Ewald. Record Office, Lnndoa.
MINNESOTA. J. G. Pyle, St Paul, Minn,
MINSTREL. Prof. Minto.
MINT. W. Chandler Roberts, F.R.S., and R. a.
Hill, both of the Royal Mint, London.
MIRABEAU. H. Morse SrapaKNe. •
MIRROR. James Paton and A. S. Murray.
MISHNAH. S. M. Sohillbb-Szinessy.
MISSAL. Rev. J. Sutherland Black, M.A.
MISSIONS. Rev. G. F. Maolear, D.D., Warden ol
St Augustine College, Canterbury.
MISSISSIPPI (River). Col. H. L. Abbot, U.S.
Engineers.
MISSISSIPPI (State). Piof. R. B. Fulton, Univereily
of Mississippi, Oxford, Misii.
MISSOURI. Prof. M. S. Snow, Washington Univereity,
St Louis, Mo.
MITE. A. D. Michael, F.R.M.S.
MOAB. Prof. Julius WELLHAUSEif, University 0'
Halle.
MOHAJIMEDANISM—
Mohammed. Prof. WELLHAUshA".
Eastern Caliphate. Prof. Stanislas Guyard.
Koran. Prof. NOldeke.
MOLE. Surgeon-Major DoBsoN, F.R.S.
MOLECULK Rev. H. W. Watson, M.A., Rector ol
Berkeswell, Warwickshire^ S. H. Bdrbury, M.A.,
Lincoln's Inn, and Prof. A. Ckum Brown.
MOLIERE. And. Lano, Author of "Helen of Troy."
MOLLUSCA. E. Ray Lankester, F.R.S., Professor
of Zoology, University College, London.
MOLOCH. Prof. W. Robertson Smith.
MONACHISM. Rev. R. F. Littledale, LL.D., D.C.L.
MONEY. C. F. Bastable, M.A., Prof, of Jurisprudence
and Political Economy, Queen's College, Galway.
MONGE. Prof. Arthur CaylBy, LL.D., 6.C.L., F.ks.
MONGOLS. R. K. Douglas, Professor of Chinese,
King's College, London, and Prof. B. JilLO, Univer-
sity of Innsbruck.
MONMOUTH, DUKE OF. Osmund Airy.
MONROE. Prof. Freeman Snow, Harvard Univereity.
Cambridge, Mass.
MONSTER. Charles Creiohton, M.A., M.D.
MONTAIGNE. Geo. Saintsbury.
MONTANA. Henry Ganneit, Geographical Depart-
ment, Washington.
MONTANISM. Prof. Harnack.
MONTENEGRO. H. A. Webster.
MONTESQUIEU. G. Saintsbury.
MONTREAL. Prof. Danifl Wilson, LL.D.
MONTROSE, MARQUIS OF. S. R. Gardiner,
■ Professor of Modern History, King's College, London.
MOON. Simon Newcomb, Professor of Astronomy,
U.S. Naval Observatory, Washington.
MOORE, SIR JOHN. H. M. Stephens.
MOORE, THOMAS. Prof. Minto.
MORAVIA. J. F. Muirhead, Leipsic.
MORAVIAN BRETHREN. Prof. 'T. JF. Lindsay, D.D.
MORE, HENRY. Very Rev. John Tui,looh, D.U.,
late Principal of St. Mary's College, St Andrews.
MORE, THOSIAS. Kev. Mark Pattison, "B.D.,
Rector of Lincoln College, Oxford.
MORMONS. Prof. John Fraseb, University of Chicago.
MOROCCO. H. A. Webster.
MORPHOLOGY. Patrick Geddes, F.R.S.E.
MORSE. Rev. S. Ibkn«ds Prime, D.D., Author of
"Life of Morse."
MORTGAGE. Edmund Robertson, LL.D., M.P., Pro-
fessor of Roman Law, University College, London.
MOSAIC. J. H. Middleton.
MOSCOW. P. A. Kropotkinb.
MOSES. Prof. Wellhausbn.
MOSES OF CHORENE. Prof. A. VON GoTBcnMir,
University of Tubingen.
MOSQUE. J. H. Middleton.
MOSQUITO. R. M'LAcni.AN, F.R:a.
^!ofreVe;;Ce''bvtI.«
ENCYCLOPAEDIA BEITANNICA.
ME N-ME N
MENA, JUAN DE, one of the Italiamzmg Spamsli poeta
of the 15th century, was bom at Cordova about
Hll. We are infonned by Romero, to whom we are
indebted for almost all we know about his life, that he had
attained the age of twenty-three before he began to give
himself to "the sweet labour of good learning," pursuing a
regular course of study at Salamanca and afterwards at
Rome. It was at the latter city that he first became
ao/iuainted with the writings of Dante and Petrarch, which
afterwards so powerfully influenced his own style. Having
returned to Spain, he became a "veinticuatro," or magis-
trate, of his native town, and was received as a poet with
great favour at the court of John n., being made Latin secre-
tary to the king and historiographer of Castile. He died
suddenly, in consequence of a fall from his mule, in 1456,
at Torrelajjuna, where the marquis of Samtillana, his friend
and patron, erected his monument and wrote his epitaph.
De Mena's principal work. El Laberinto {" The Labyrinth "),
Bometiities called Las Trescienlas (" The Three Hundred ")
from the original number of its stanzas, is a didactic
allegory on the duties and destinies of man, obviously con-
Btnicted on the lines of the Divina Commedia of Dante.
The poet, while wandering in a wood and exposed to the
attacks of various beasts of prey, is met by Providence in
the gtiise of a beautif iil woman, who ofiers to guide him
safely through the dangers which siuroimd him, and at the
same time to explain — " as far as they may be grasped by
human understanding" — the dark mysteries of life that
weigh upon his spirit. He is then led to the spherical
centre of the five zones, where he sees the three wheels of
destiny, the past, the futxu-e, and the present, and the men
belonging to each, arranged in the seven circles of planetary
influence. Opportunity is thus afforded for a vast quan-
tity of mythological and historical portraiture ; the best
sketches are those of the poet's own contemporaries, but
the work in general is much disfigured with all sorts of
pedantry, and hardly ever attains to mediocrity as a poem.
The Laberinto was first printed at Seville in 1496 ; Nunez
and Sanchez accompanied it iitith commentaries in 1499
and 1582 respectively ; and it is stiU regarded with a good
deal of reverence by the Spaniards as the " magnum opus "
of their " Enhius." De Mena was the author of a number
of minor poems or " vers de soci^t^," .written merely for
IC— 1
court circles, and having neither general interest nor per-
manent value; most of them are to be found in the
Cancionero General. He also wrote a poem entitled La
Coronacion, the subject being the "crowning" of the
marquis of Santillana by the Muses and the Virtues oa
Mount Parnassus. Finally, his Sietc Pecados Motialet
(" Seven Deadly Sins ") is a dull allegory on the antagonism
between reason ■ and the • vi'ill of man. Complete editions
of the poems of De Mena appeared in 1528, 1804, and
1840.
MfiNACE, GiLLEs (1613-1692), described by Bayle as
" one of the most learned men of his time, and the Varro
of the 17th century," was the son of GuUlaume Manage,
king's advocate at Angers, and was bom in that city, on
August 15, .1613. A tenacious memory and an early
developed enthusiasm for learning carried him speedily
through his literary and professional studies, and we read
of him practising at the bar at Angers as early as 1632.
In the same year he pleaded several causes before the
parlement of Paris, and soon afterwards he attended the
" Grand Tours " at Poitiers, but after having been laid
aside by a severe illness he abandoned the legal profession
and declared his intention of entering the church. He
succeeded in obtaining some sinecure benefices, and lived
for some years in the household of Cardinal De Retz (then
only coadjutor to the archbishop of Paris), where he had
ample leisure for his favourite literary pursviits.- Some
time after 1648 hfe withdrew to a house of his own in the
cloister of Notre Dame, where his remarkable conversational
powers enabled him to gather round him on Wednesday
evenings those much frequented literary assemblies which
he called. " Mercuriales." His learning procured for him
admission to the Delia Crusoan Academy of Florence, but
his irrepressible tendency to caustic sarcasm led to his
remorseless exclusion from the French Academy. He died
at Paris on July 23, 1692. Of the voluminous works
of Manage (fully enumerated in the Dictiannaire of
Chauffepi^) the following may be mentioned : — Oriffinet
de la Langue Fran^oise (1650 ; greatly enlarged in 1694) ;
Diogenes Laertim Grace et Latine, cum CommerUario (1663
and again much improved in 1692); Poemata Latina,
Gallica, Grsica, et Italica (1656; 8th ed., 1687); Originx
delta Lingua luUiana (1669); and Anti-BaiUet (1690).
^
M- E N — M E N
Alter his death a volume of Menagiana was published ; it
was afterwards expanded into two, and, with great addi-
tions, into four in the Paris edition of 1715.
MENANDEK, the most famous Greek poet of 'the
New Comedy, which prevailed from about the death of
Alexander the Great (323 B.C.) to 250. He was bom at
Athens in 342, and died, it was said, by drowning in the
harbour of that city (Piraeus) in 291. His social tastes
induced him to write plays rather for the upper classes,
and to raise comedy to a gentility which it had hardly
possessed in the hands of the preceding comic poets. Ho
was the associate, if not the pupil, of Theophrastus, who
himself had been a disciple of Plato and Aristotle, and he
was the intimate friend and admirer of Epicurus ; but he
also enjayed the more distinguished patronage of Demetrius
Phalereus (who was likewise a pupil of Theophrastus), and
of Ptolemy the son of Lagus.^ His principal rival in the art
was Philemon, who appears to have been more popular with
the multitude, and for that reason probably more successful.
It is said that out of a hundred comedies Menander gained
the prize vrith but eight. All the extant plays of Terence,
with the exception of the Phormio, are avowedly taken
from Menander ; but some of them appear to have been
adaptations and combinations of more than one plot,
although Terence himself says in the prologue to the
Adelphi (11) that he copied the Gree^ model clesely,
"vorbum de verbo expressum extulit." Jvdius Caesar
called Terence dimidiatus Menander, as if two halves of
different plays had been fitted into one.^
The Attic New Comedy, says Dr Wagner,^ "may be
designated as essentially domestic," i.e., as opposed to
that free discussion of the politics of the day which gave
to the Old Comedy the place which is held by the " leading
articles " of a modern newspaper. " The stock characters
were such as the stem or weak father, the son whose
follies are seconded by a slave or a hungry parasite, the
pettifogger, active in stirring up law suits, and the gascon-
ading soldier of fortune." ^ These and cognate subjects,
which formed the stock-in-trade of Menander's plays, are
summed up in two well-known lines of Ovid — -.
"Dum fallax servu3, dunis pater, improba lena-
Vivet, dum meretrix blanda, Menandros erit."
It 13 a good remark of Dr Wagner's ^ that the last-mentioned
of Ihese, the meretiix blanda (which probably refers
especially to the Thais), "holds the most important" and
conspicuous part in the New Attic Comedy, while married
ladies are continually represented as the plague and bore
of their husbands' lives." Intrigues ivith these, generally
through the medium of a clever confidential slave, are for
the most part the very point or- pivot on which the j)lot
turns.
The more literary Romans greatly admired Menander
as a poet. Pliny {N". H., xxx. 1, § 7) speaks of him as
"Menander litterarum subtilitati sine a;mulo genitus."
Propertius, contemplating a visit to Athens,^ anticipates
the pleasure of reading Menander in his native city —
" Persequar aut studium lingute, Demostheuis arma,
Libaboque tuos, scite Menaudre, sales."
' In allusion to this Pliny writes {Jf. n.^vii. 30, § 11 1), " Magnura
et Monandro in coinico bocco testimonium rcguni JE^ypii et Mace-
tloniae coiitigit classo et per legatos petito ; niajus ex ipso, regiffi
fortunas pra;lata litterarum conscientia." This seems to say that
Mcnaudcr had been invited to tlie courts of Alexander and Ptolemy,
US Euripides had' been lo that of Archelaus, king of Macedonia, but
had preferred to write comedies for the Attic stage.
^ Thus the Andria, Jleauiontimorumino^, and Hccyra. are described
Bevcrally in the tituli prefixed as Qrwca or tola Orteca Mcnandru.
The liunuch and Timorumen.08 are each based on two plays of
Menander, and the Adelphi was compiled partly from Menander and
partly from Diphilus.
• Introduction to Terbnce, p. 6 fBell, 1860).
* Professor Jebb, Primer of Qredk Literature, p. 101.
» m sup., p. 7. ' El., iv. 21 27.
He elsewhere speaks of him as "mundus Menander,
neat, terse, and lu-bane; and his skill in depicting th«
character of a fascinating Thais is alluded to here and
in ii. 6, 3 : —
** Turba Menandreie fuerat ncc Tlraidos olim
Tanta, in qua populus lusit Erichtboiiius."
'Of this comedy, the Tliais, Professor MahaSy remarks
that- perhaps it was the most brilliant of Menander's plays.
" the manners and characters of the personage being painted
with thorough experience as well as genius." Nevertheless,
only five verses of this play have been preserved to us, one
of which is that quoted by St Paul (1 Cor. xv. 33), "Evil
communications corrupt good manners." The same critic,
in praising Menander's stylo as the purest model of the
New Attic, observes that a remarkable feature of the New
Comedy was " its utter avoidance of rhetoric " (p. 489).
The influence which this art had on Euripides is well
known. Sophocles was not whoUy exempt from a kind of .
rhetorical pedantry, and the speeches in Thucydides are
so many exercises of the author in that art. But, as
rhetoric pertained essentially to public life, it was likely
to have a much less scope in scenes borrowed almost solely
from social and domestic experiences.
Menander, however, did not neglect the other branch of
a liberal Attic education, — phOosophy. A follower and a
friend of Epicurus, whose summum bonum was the greatest
amount of enjoyment to be got out of life, he carried out
in practice what . he advocated by precept ; for he was
essentially the well-to-do gentleman,^ and moved in the
upper circles of Athenian society. " The philosophers of
the day " {i.e., the schools and universities in our modern
systems of teaching) " were still," says Professor Mahaffy,'
viz., even during the period of the New Comedy, " the con-
stant butt of the dramatists." He adds that, " what is
still stranger, political attacks on living personages, not
excepting Alexander the Great, were freely .and boldly
made."
On the whole, our estimate of the spirit and object of Menander
must be formed rather from bis imitator and copyist Terence than
from the fragments which remain, about 2400 verses in all, as col-
lected by Meineke in bis Fragmcnia Comicorum Ormcontm. For,
as Professor MahafFy vrell observes,^" tho extracts made by
Athenseus, our principal authority, have reference chiefly to "the
arcbaiology of cooks and cookery," while Stobaus was a collector of
■yvoj^ai or wise maxims, — "a most unfortunate and worthless kind
of citation. " It follows that no sound conclusions as to dramatic
genius, or of the knowledge of human nature, can be drawn from
detached i-erses preserved without the least reference to these par-
ticular points. The exb-aordinary popularity of Menander must
have been due to literary merh, if not to great originality. Mr
Mabaffy observes on this" that " there is so much of a calm gentle-
manly morality about his fragments, be is so excellent a t4:acher
of the ordinary world-wisdom — resignation, good temper, modera-
tion, friendliness— that we can well understand tl<.is popul.'.ri Sy.
Copies of his plays continued loug in existence, and were cert-uulj-
known to Suidas and Eustathius as late as tho 11th and 12th cen-
tmics, if they did not survive to a yet later period.'*'
In respect of language, Menander occupies the same position in
poetry wliich his contemporary Demosthenes does in prose. In botli
the New Attic is elaborated with great finish, and with much greater
grammatical precision than wo find in WTitcrs of the Old Attic, such
as Sophocles and Thucydides, A considerable addition to the
vocabulary of evcry-day life had now been nuide, aa was indeed
inevitable from the veraitile character of the language and the
genius of the people who used it. Many new verb-forms, cspccialk
the perfect active," now occur, and indeed form a characteristic
innovatnou of tho style of Plato, The earlier prose was in its
general vocabulary to a considerable extent jioetical. and such a
concurrence of short syllables as in tho Platonic diroScSoKijaaK^Tcr
\
7 Hist. Class. Gr. Lit., i. p. 483.
* Pliny calls Menander "diligeuti^simus lururiSB intcrprcs," N. //.,
xxxvi. 5.
" ilist^ Clcvss. Gr, Lit., i. p. 480.. ^° Ibid., p. 480.
" Ibid., p. 487. " Ibid., p. 490.
^^ A curious example ia airfHrdyKafftt the -transitive perfect of
iLvoKTtlvtiy. Stniilarly we hare the unnsQal forms K4xpVita (fragp
'559), i^p6<pnKa {"^^y), ffiryK^Xi"** (810).
MENDELSSOHN
in thickness " anything he had attempted. From letters
written at this period we leam that Felix's estimate of the
French school of music was very far from a flattering
one • but he formed some friendships in Paris, which
were pleasantly renewed on later occasions. He returned
to Berlin with his father in May 1825, taking leave of
his Parisian friends on the 19th of the month, and
interrupting his journey at Weimar for the piu-pose of
myin" a second visit to Goethe, to whom he dedicated his
quartctt in B minor. On reaching home he must have
fallen to work with greater zeal than ever; for on the
23d of July in this same year he completed his pianoforte
capriccio in F sharp minor (Op. 5), and on the 10th of
August an opera, in two acts, called Die Ilochseit des
CamacJi.0, a work of considerable importance, concerning
which WB shall presently have to speak more particularly.
No ordinary boy could have escaped uninjured from
the snares attendant upon such a life as that which
Mendelssohn now lived. Notwithstanding his overwhelm-
ing passion for music, his general education had been so
well cared for that he was able to hold his own, in the
society of his seniors, with the easy grace of an acec jnplishcd
man of the world. He was already recognized as a lead-
ing spirit by the artists with whom he associated, and
these artists were men of acknowledged talent and position.
Vhe temptations to egoism by which he was surrounded
would have rendered most clever students intolerable. But
the natural amiability of his disposition, and the healthy
influence of his happy home-life, counteracted aU tendencies
towards- inordinate self-assertion ; and he is described by
all who knew him at this period as the most charming
boy imaginable. Even Zelter, though by nature no less
repressive than Cherubini,- was not ashamed to show that
he was proud of him; and Moscheles, whose name was
already famous, met him from the first on equal terms.
Soon after his return from Paris, Abraham Mendelssohn
removed from his mother's residence to No. 3 Leipziger
Strasse, a roomy, old-fashioned house, containing an
excellent music-room, and in the grounds adjoining a
" Gartenhaus " capable of accommodating several hundred
persons at the Sunday performances.^ In the autumn
of the following year this "garden-house" witnessed a
memorable private performance of the work by means of
which the gi-eatness of Mendelssohn's genius was first
revealed to the outer world — the overtm-e to Shake-speare's
Midsummer Night's Dream. Tlie finished score of this
famous composition is dated "Berlin, August 6, 1826," —
that is to say, three days after its author had attained the
age of seventeen years and a half. Yet we may safely
assert that in no later work does he exhibit more originality
of thought, more freshness of conception, or more perfect
mastery over the detaUs of technical construction, than
in this delightful inspiration, which, though now nearly
sixty years old, still holds its place at the head of the most
brilliant achievements of our modem schools. The over-
ture was first publicly performed at Stettin, in February
J1827, under the direction of the young composer, who
with this bright patent of artistic nobility to support his
daim, was at once accepted as the leader of a new and
highly characteristic manifestation of the spirit of modem
progress. Henceforth therefore we must speak of him, not
as a student, but as a mature and experienced artist.
Meanwhile Camacho's Wedding had been submitted to
Hcrr General-Musik-Director Spontini,- with a view to its
production at the opera. The libretto, founded upon an
episode in the history of Don Quixote, was written by
Klingemann, and Mendelssohn threw himself into the spirit
'' ^ After MendelBSohn's death this hoose was sold to the Fmasiau
Govenimeiit ; and tho " Herrenhaas " now stands on the site of the
garden-boQSc.
of the romance with a keen perception of its peculiar
humour. The work was put into rehearsal soon ajfter the
composer's return from Stettin, produced on April 29,
1827, and received with great apparent enthusiasm; but,
for some reason which it is now impossible to ascertain,
a cabal was formed against it, and it never reached a second
performance. The critics abused it mercilessly; yet it
exhibits merits of a very high order. The solemn passage
for the trombones, which heralds the first appearance of
the knight of La Mancha, is conceived in a spirit of
reverent appreciation of the idea of Cervantes, which
would have done honour to a composer of lifelong
experience. Even the critics suborned to condemn the
work could not refrain from expressing their admiration
of this; but it had been decreed that the opera should
not live — and it did not.
Mendelssohn was excessively annoyed at tliis injustice,
and sorne time elapsed before his mind recovered ite usual
bright tone ; but he continued to work diligently for the
cause of art. Among other serious imdertakings, he
formed a choir for the study of the great choral works
of Sebastian Bach, then entirely unknov.-n to the public ;
and, in spite of Zelter's determined opposition, he suc-
ceeded, in 1829, in inducing the BerUn Singakademie
to give a public performance of the Passion according to
St Matthew, under his direction, with a chorus of between
three and four hundred voices. The scheme succeeded
beyond his warmest hopes, and proved the means of
restoring to the world great compositions with which we
are all now familiar, but which, at that time, had never been
heard since the death of Bach. But the obstructive party
were grievously offended ; and at this period Mendelssoha
was far from popular among the musicians of Berlin
In April 1829 Mendelssohn paid his first visit lO
London. His reception was most enthusiastic. He made
his first appearance before an English audience at one of
the Philharmonio Society's concerts — then held in the
Argyll Rooms — on the 25th of May, conducting his
symphony in C minor from the pianoforte, to which he was
led by John Cramer. On the 30th he played Weber's
ConccrtstUck, from memory, a proceeding at that time
extremely unusuaL At a concert given by Drouet, on the
24th of June, he played Beethoven's pianoforte concerto in
E flat, which had never before been heard in the country ;
and the overture to A Midsummer Night's Dream was also,
for the first time, presented to a London audience. On
returning home from the concert, Mr Attwood, then
organist of St Paul's Cathedral, left the score of the
overture in a hackney coach, whereupon Mendelssohn
wrote out another, from memory, without an error. At
another concert he played, with Moscheles, his still un-
published concerto in E, for two pianofortes and orchestra.
After the close of the London season" he started with
Klingemann on a tour through Scotland, where he was
inspired with the first idea of his overtiu-e to The Isks
of Fingal, returning to Berlin at the end of November:
Except for an accident to his knee, which lamed him for
some considerable time, his visit was a highly successful
one, and laid the fotmdation of many firm friendships and
many prosperous negotiations in the time to come.
The visit to England formed in reality the first division
only of a great scheme of travel which his father wished
him to extend to all the most important art centres in
Europe. After refusing the offer of a professorship at
Berlin, he started again, in May 1830, for Italy, pausing
on his way at Weimar, where he spent a memorable fort-
night with Goethe, and reaching Rome, after many pleasant
intemiptions, on November 1. No possible form of
excitement ever prevented him from devoting a certain
time every day to composition ; but he lost no opportunitj;
B
MENDELSSOHN
of studying either the countless treasures which form the
chief glory of the great city of the manners and customs of
modern Romans. He attended, with insatiable curiosity,
the services in the Sistine Chapel ; and his keen power of
observation enabled him to throw much interesting light
upon thera. His letters on this subject, however, lose
much of their value through his incapacity to comprehend
the close relation existing between the music of Palestrina
and his contemporaries and the ritual of the Roman
Church. His Lutheran education kept him in ignorance
even of the first principles of ordinary chanting; and it
is amusing to find him describing as enormities peculiar
to the papal choir customs familiar to every village singer
in England, and as closely connected with the structure of
the " Anglican chant " as with that of " Gregorian music."
Still, though he could not agree, in all points, with Baini,
the greatest ecclesiastical musician then living, he fuUy
shared his admiration for the Jmproperia, the Miserere, and
the cantiis planum of the Lamentationes and the Emdtet,
the musical beauty of which ho could understand, apart
from their ritual significance.
In passing through Munich on his return in October 1831,
he composed and played his pianoforte concerto in G minor,
and accepted a commission (never fulfilled) to compose an
opera for the Munich theatre. Pausing for a time at
Stuttgart, Frankfort, and Diisseldorf, he arrived in Paris
in December, and passed four pleasant mouths in the
renewal of acquaintances formed in 1825, and in close
intercourse with Liszt and Chopin. On February 19,
1832, the overture to A Midsv.mm.sr Night's Dream was
played at the conservatoire, and many of his other com-
j.ositions were brought before the public ; but he did not
!,itogether escape disappointments with regard to some of
them, especially the Reformation symphony, and the visit
was brought to a premature close in March by an attack
nf cholera, from which, however, he rapidly recovered.
On the 23d of April 1832 ho was again in London,
where he t\vice played his G minor concerto at the
Philharmonic concerts, gave a performance on the organ
it St Paul's, and published his first book of Lieder ohne
Worte. He returned to Berlin in July, and during the
winter he gave public performances of his Reformation
symphony, his concerto in G minor, and his Walpur-
gisnacht. In the following spring he paid a third visit
to London for the purpose of conducting his Italian
symphony, which was played for the first time, by the
Philharmonic Society, on the 13th of May 1833. On the
26th of the same month he conducted the performances at
the Lower Rhino festival at Diisseldorf, with such brilliant
effect that he was at once in'.-ited to accept the appointment
of general-music-director to the town, an office which
included the management of tho music in the principal
churches, at the theatre, and at the rooms of two musical
associations. This post he willingly accepted, and it formed
a stepping-stone to a far more important one.
Before entering upon his now duties, Mendelssohn paid
B fourth visit to London, with his father, returning to
Diisseldorf on the 27th of September 1833. His iiilluenco
produced an excellent effect upon the church music and in
tho concert-room ; but his relations with tho 'management
of the theatre wore not altogether pleasant ; and it was
probably this circumstance which first led him to forsake
the cultivation of the opera for that of sacred music. At
Diisseldorf he first designed his famous oratorio St Panl,
in response to an application from tho Ciicilien-Vcvcin at
Frankfort, composed his overture to Die schiitie Mrlusine,
and planned some other works of importance. He liked his
appointment, and would probably have retained it much
longer had he not been invited to undertake the permanent
direction of the Oowandhaus concerts at Leipsic, and thus
raised to the highest position attainable in the Gemma
musical world. To this new sphere of labour he removed
in August 1835, opening the first concert at the Gewand-
haus, on the 4th of October, with his overture Die
Meeresstille, a work possessing great attractions, though
by no means on a level with the Midsummer NigMt
Dream, The Isles of Fingal, or Melusine.
Mendelssohn's reception in Leipsic was most enthusiastic;
and under their new director the Gewandhaus concerts
prospered exceedingly. Meanwhile St Paid steadily pro-
gressed, and was first produced, with triumphant success,
at the Lower Rhine festival at Diisseldorf, on May 22,
1836. On October 3 it was first sung in English, at
Liverpool, under the direction of Sir George Smart ; and
on March 16, 1837, Mendelssohn again dii-ected it at
Leipsic.
The next great event in Mendelssohn's life was his happy
marriage, on March 28, 1837, to Cecile Charlotte Sophie
Jeanrenaud, whose amiable disposition, surpassing beauty,
and indescribable charm of manner endeared her to all
who knew her. The honeymoon was scarcely over before
he was again summoned to England to conduct St Paid,
at the Birmingham festival, on September 20th. During
this visit he played on tho organ at St Paul's and at
Christ Church, Newgate Street, with an effect which
exercised a lasting influence upon English organists. It
was here also that he first contemplated tho production
of his second oratorio, Elijah.
Passing over the composition of the Lohgesang in 1S40,
a sixth visit to England in the same year, the scheme for
the erection of a monument to Sebastian Bach, and other
events on which space does not permit us to enlarge, we find
Mendelssohn in 1841 recalled to Berhn by the king of
Prussia, with the title of Kapellmeister. Though this
appointment resulted in the production of Antigone, CEdipus
Coloneus, Aihalie, the incidental music to the Midsummer
Nights Dream, and other great works, it proved an endless
source of vexation, and certainly helped to shorten the com-
poser's life. In 1842 he came to England for the seventh
time,- accompanied by his wife, conducted his Scotch
symphony at the Philharmonic, again played the organ at
St Peter'.s, Cornhill, and Christ Church, Newgate Street,
and v/as received with all possible honour by the queen and
the prince consort. He did not, however, permit ]iis new
engagements to interfere with the direction of the Gewand-
haus concerUi ; and in 1843 he founded in Leipsic the great
conservatoire which soon became the best musical college
in Europe, opening it on April 3, in the buildings of the
Gewandhaus. In 1844 he conducted six of the Philhar-
monic concerts in London, producing his new Midsummer
Xighi's Dream music, and playing Beethoven's pianoforte
concerto in Q with extraordinary effect. Ho returned to
his duties at Berlin in September, but liappily succeeded
in persuading tho king to free him from his most onerous
engagements, and his delight at this relief was un-
bounded.
After a brief residence in Frankfort, Mendelssohn
returned to Leipsic in September 1845, resuming his
old duties at the Gev/andhaas, and teaching regularly
in tho conservatoire. Here he remained, ^vith little in-
tcrniption, during tho winter, — introducing his friend
Jenny Liud, then at the height of her popularity, to
the critical frequenters of the Gewandhaus, and steadily
working at Elijah, the first performance of which he con-
ducted at the Birmingham festival, on August 26, 1846.
The enthusiastic reception of this great work is well known.
Unhappily, the excitement attendant upon its production,
added to the irritating effect of tho worries at Berlin, made
a serious inroad upon the composer's health. On his
return to Leipsic ' ho worked on as usual, but it was
M E N — M E N
clear that his health was serioosly impaired In 1847 he
visited England for the tenth and last time, to conduct four
performances of Elijah at Exeter Hall, on the 16th, 23d,
28th, and 30th of April, one at Manchester on the 20th,
and one at Birmingham on the 27th. Again the queen
and prince consort received him with marked respect, —
one might almost venture to say, affection, — and all seemed
prosperous and happy. But the necessary exertion was
far beyond his strength. He witnessed Jenny Lind's first
appearance at Her Majesty's Theatre, on the 4th of May, and
left England on the 9th, little anticipating the trial that
awaited him in the tidings of the sudden death of his sister
Fanny, which reached him only a few days after his arrival
in Frankfort. The loss of his mother-in 1842 had shaken
him much, but the suddenness with which this last sad
intelligence was communicated broke him down com-
pletely. He fell to the ground insensible, and never fully
recovered. In June he was 'so far himself again that he
was able 'to travel, with his family, by short stages, to
Interlaken, where he stayed for some time, illustrating
the journey by a series of water-colour drawings, but
making no attempt at composition for many weeks. He
returned to Leipsic in September, bringing with him
frag'ments of Christxts, Lorelei/, and some other unfinished
works, taking no part in the concerts, and living in the
strictest privacy. On the 9th of October he called on
Madame Frege, and asked her to sing his latest set of songs.
Sh^ left the room for lights, and on her return found him
in violent pain, and almost insensible. It was the begin-
ning of the end. He lingered on, now better now worse,
through four weary weeks, and on the 4th of November
he passed away, in the presence of his wife, his brother,
and his three dear friends, Moscheles, Schleinitz, and
Ferdinand David. A cross nov marks the site of his
grave, in the Alte Dreifaltigkeits Kirchhof, at Berlin.
Mendelssohn's title to a place among the greatest composers of
the c«ntury is incontestable. His style, though differing bnt little
in technical arrangement from that of his classical predecessors, is
characteriied by a vein of melody peculiarly hi3 own, and easily
distinguishable by those who have studied his vioxVa, not only
fh)m the genuine effusions of contemporary writers, but from tJie
most successful of the servile imitations with which, even during
his lifetime, the music-shops were deluged. In less judicious hands
the rigid symmetry of his phrasing might, perhaps, have palled
apou the car ; but under his skilful management it serves only to
impart an additional charm to thoughts which derive their chief
beauty from the evident spontaneity of their conception. In this,
as in all other matters of a purely technical character, he regarded
the accepted laws of art as the medium by which he might most
certainly attain the ends dictated by the inspiration of his genius.
lliongh caring nothing for rules, except as means for producing
a good effect, he scarcely ever violated them, and was never weary of
impressing their value upon the minds of his pupils. His method
of counterpoint was modelled in close accordance with that practised
by Sebastian Bach. This he used in combination with an elastic
development of the sonata-form, similar to that engrafted by
Beethoven upon the lines laid down by Haydn. The principles
involved in this arrangement-were strictly conservative ; yet tney
enabled him, at the very outset of hia career,"to invent a new style
no less original than that of Schubert or Weber, and no less re-
markable as the embodiment of canons already consecrated by
classical authority than as a special manifestation of individual
^nins. It is thus that Mendelssohn stands before us as at the same
time a champion of conservatism and an apostle of progress ; and
it is chiefly by virtue of these two apparently iucongnious though
really perfectly compatible phases of his artistic character that his
influence and example have, for so many years, held in check tlie
violence of rea<;tionary opinion which a littlb injudicious en-
couragement might easily have fanned into revolutionary fury.
Happily, this wholesome influence is still at work among us ; and
in his oratorios, his symphonies, his overtures, his concertos, and
his smaller pianoforte pieces Mendelssohn sets before us an ex-
ample the value of which is univarsally recognized, and not likely to
be soon forgotten.
I Concerning Mendelssohn's private character there have never
l)cen two npmions. As a man of the world, ho was more than ordi-
"carily accomplished, — brilliant in conversation, and in his lighter
momenta overflowing with sparkling humour and ready pleasantry,
loyal and unselfish in the more serious bnsinesa of life, and never
weary of working for the general good. As a friend he was un-
varyingly kind, sympathetic, and as tree as steel. His earnestness
as a Christian needs no stronger testimony than that afforded by
his own delineation of the character of St Paul ; but it is not too
much to say that his heart and life were pure as those of a little
child.
A complete list of Mendelssohn's published compositions— «ne hundred and nine-
teen In number, besides some flvo and twenty unnnmbercd Troilu of considerable
Importance — will be found In the-themnllc catalogue published by Hesara Brelt-
kopf and Hartel at Lelpslc, ond also In Grove's Dictionai-y of Muaie and
Muiicians, vol U, pp. 3«8, 309. Among bis miscellaneous writings, we mny men-
tion a translation of the Andria of Terence, In German wrso, and on Immense
collection of letters, po9tlinmou5ly printed, and calculated to give the reader
a for closer acquaintance with his life and character than any bloeru];ilier can hope
to convey. (w. S. R.)
MENDELSSOBLN, Moses (1729-178G), philosopher
and scholar, well kno'wn as Lessing's friend and the proto-
type of his "Nathan," was bom on September 6, 1729, at
Dessau on the Elbe, where his Jewish father made a scanty
livelihood by teaching a small school and transcribing
copies of the " law." The leading events of Mendelssohn's
career have been indicated elsewhere (see Jews, vol iHii,
p. 680). His numerous writings include Ueber Evident
in metaphysischen Wissenschaften, (1763), which gained
the prize in a competition in which Immanuel Kant took
part; Brief e iiber die Empjinduitff en (1764) ; Phxdon, oder
iiber die UiisierblicMxit der Seele (1767), an argument foi
immortality, founded on the nature of the soul as exempt-
ing it from the ordinary laws of change, which has been
severely criticized by Kant ; Jerusalem, oder die religiiist
AfachtundJudentkum (1783), a specially important con-
tribution to the question of Jewish emancipation ; a
number of contributions to his friend Nicolai's Literatur-
brie/en and Bibliothek der schijnen Wissenscha/ten ; one or
two tracts in Hebrew ; and some new German translations
from the Old Testament. The controversy which led to
the publication of his Morgenslunden (1785-86), a reply
to Jacobi's Brief e iiber die Lehre Spinoza's, is said to have
been more or less directly the cause of his death, which
took place on January 4, 1786 (see Jacobi, vol. xiii. p.
537). Of Mendelssohn's three sons, the second, Abraham,
settled as °a banker in Hamburg and married a Jewess, Lea
Salomon Bartholdy, who bore him four children ; these, by
advice of their mother's brother, himself a conscientious
convert from Judaism, were educated as Christians, and
thenceforth joined their mother's second surname to their
oivn. The second of them, Felix, is the subject of the
preceding notice. In later life Abraham Mendelssohn
was accustomed to say, — " When I was young I was the
son of my father ; now I am the father of my son." See
The Mendelssohn Family, 1882.
MENDOZA, a city of the Argentine Eepublic, the only
town of the province of Mendoza, lies 700 miles west-
north-west of Buenos Ayres, at the foot of the Cordilleras,
2510 feet above the sea-level, in 32° 63' S. lat. and 68° 45'
W. long. It ivas formerly a frequent stopping-place on the
route across the Andes by the Uspallata Pass, and used to
rank as one of the best-built to'wns in the country, but in
1861 it was almost completely destroyed by an appalling
earthquake, in which the people, for the most part
collected in the churches, perished to the number of
about 12,000. Bravard, a French geobgist who had often
predicted the catastrophe, was one of those wlio perished.
Extensive ruins still mark the site of the old town ; the
new toivn, which has been built at a little distance, has
grown rapidly. Situated in a richly cultivated district,
Mendoza deoends mainly on agriculture and fruit-growing.
The city was founded in 1559 by Garcia de Mendoza; and in
1776 it was made the administrative centra of the vioc-royalty of
La Plata. See Mulhall, Handbook of the La Plata Stales, 1875;
and Mre Mulhall, Between the Amazon and the Andes, 1881i.
MENDOZA, Diego Huetado de (c 1503-1575).
novelist, poet diplomatist, and historian, ■was a younger son
of the membet of the illustrious Mendoza family to whom
XVL — 2
10
M E N — M E N
tho government rj Granada tvbs entrusted not Ibng after ita
RitrTfinder, and was born in that city about the year 1503.
The marquis of SantiUana, so prominent a figure at the court
of John II. of Castile, was his great-grandfather. At an
early age Mendoza, who had been destined for the church,
was sent to Sahimanca, where he studied with success, and
also, some time between the years 1520 and 1525, produced
his Lazarillo de Tormes, the work upon which his literary
celebrity largely rests. Having persuaded his father to
allow him to enter the army, he served with the Spanish
troops of Charles V. in Italy, and also availed himself of
opportunities as they arose to hear tho lectures of famous
professors at Bologna, Padua, and Rome. In 1538 he was
taken into the diplomatic service of the emperor and sent as
ambassador to Venice ; there he cultivated friendly relations
with the Aldi, and energetically set about collecting a
library, not only procuring copies of many old MSS. in
the public library of the city, but also sending to Thessaly
and Mount Athos for new ones ; it was from his collection
that the complete text of Josephus was first printed. For
some time he held the post of military governor of Siena ;-
and, after having been present in an official capacity in
Trent at the beginning of the cecumenical council, he was in
1547 sent as special plenipotentiary to Kome, where he
continued to act for some years. In 1554, shortly before
the abdication of Charles, he was recalled to Spain, and his
official career came to an end. He was never a favourite
with Philip n. ; and in consequence o£ a quarrel with a
courtier, in which he had lost his temper badly, he was
finally banished from court in 1568. The remaining years
of his life, which were spent at Granada, he devoted partly
to the study of Arabic, partly to poetical composition, and
partly to the preparation of his history of the Moorish
insurrection of 1568-70 {Guerra de Granada).. He died
at Madrid (which he had obtained leave to visit on some
business en"and) in April 1575.
Mendoza's Lazarillo dc Tormes, though written during his
college days, was not published until 1553, when it was printed
anonymously at Antwerp. Next year it was reprinted at Burgos,
but ultimately it was taken exception to by the Inquisition, and the
Spanish editions of 1573 and subsequent years are accordingly con-
siderably abridged. It is a comparatively short fragment, written
in vigorous and bright Castilian, and was the first example in modem
literature of the " novela picaresca" of which Le Sage's Oil Bias
now ranks as the most perfect specimen. The continuations, first
by an anonymous author (1555) and afterwards by H. dp Luna (1620),
are of very inferior interest Of Mendoza as a poet all that need,
be said hero is that ho followed the modem Italian models quite as
far as was compatible with a due regard to his Castilian individu-
ality. His history, though of no great bulk, is, hke his novel, a
work of remarkable literary execution. It relates indeed only to a
eomparatirely brief episode in a chapter of events for which it is
almost impossible to claim much general attention, ,and it is often
needlessly erudite and sometimes provokingly obscure. But as a
whole itis singularly well-informed, dignified, and picturesque ; " the
style is bold and abi-upt, but true to the idiom of the language, and
the current of thought is deep and strong, easily caiTying the reader
onward with its flood. Nothing in the old chronicling style of the
earlier period is to be compared to it, and Uttle in any subsequent
period IS equal to it for manliness, vigour, and truth " (Tickno:-).
The first edition of the Giurra de Granada did not appear until
1610, hut was even then incomplete ; the first perfect edition was
that of 1730. The work has frequently been repnnted since.
MENDOZA, Iniqo Lopez de. See SiNTiLLAffA.
MENELAUS, king of Sparta, was tho brother of
Agajcemnon {q.v.) and tho husland of Helena {q.'o.). He
was one of the heroes of the Trojan horse, and recovered
Uis wife at the sack of the city. On the voyage home-
wards his fleet was scattered o£E Malea by a storm which
drove him to Crete ; after seven years' further wandering
to Cyprus, I'hrordcia, Egypt, Ethiopia, Libya, and the
fcountry of the Erembi, he at last had an interview with
Proteus and obtained a favourable \\'ind which brought him
home on tho very day on which Orestes was holding the
funeral feast over ^gisthus and Clytnemnestra. After a
long and happy life in Lacedsemon, Menelaus, as the son-
in-law of Zeus, did not die but was translated to Elysium.
MENGS, Antony Raphael (1728-1779), was the most
celebrated representative of the eclectic school of painting
in the 18th century, and played a great part in- the early
days of the Classic revival. Ho was born in 1728 at Anssig
in Bohemia, but his father, a Danish painter, established
himself finaDy at Dresden, whence in 1741 he conducted his
son to Rome. Mengs early showed that active intelligence
and large capacity for laborious study which secured him
the extraordinary distinction which he enjoyed through life.
His appointment in 1749 as first painter to the elector of
Saxony did not prevent his spending much time in Rome,
where he had married in 1748, and abjured the Protestant
faith, and where he l^ecame in 1754 director of the Vatican
school of painting, nor did this hinder him on two occasions
from obeying the call of Charles ITT of Sijain to Madrid.
There Mengs produced some of his best work, and
specially the ceiling of the banqueting hall, the subject of
which was the Triumph of Trajan and the Temple of Glory.
After the completion of this work in 1777, Mengs again
returned to Rome, and there he died, two years later, in
poor circumstances, leaving twenty children, seven of whom
were pensioned by the king of Spain. Besides numerous
paintings in the Madrid gallery, the Ascension at Dresden,
Perseus and Andromeda at St Petersburg, and the ceding
of the Villa Albani must be mentioned among his' chief
works. In England, the duke of Northumberland pos-
sesses a Holy Family, and the colleges of All Souls and
Magdalen, at Oxford, have altar-pieces by his hand. In
his -ivritings, in Sparush, ItaUan, and German, Mengs has
put forth his eclectic theory of art, which treats of per-
fection as attainable by a well-schemed combination of
diverse excellences,— Greek design, with the expression
of Raphael, the chiaroscuro of Correggio, and the colour
of Titian. His close intimacy with Winkeknanu — who
constantly wrote at his dictation — has greatly eahanced
his historical importance, for he formed no scholars, and
the critic must now concur in Goethe's judgment of Mengs
in Winkelmanri und seine Jahrhnnderi ; he must deplore
that so much learning should have been allied to a total
want of initiative and utter poverty of invention, and
embodied ■with a strained and artificial mannerism.
See Opere di Antonio Raffaello Mengs, Parma, 1780 ; Mengs'
Wcrhe, Uberseizt v. O. F. Frange, 17S6 ; Zeitschrift fUr bildtiuU
Kunst, 1880; Bianconi, Elogio Storico di Mengs, Milan, 1780;
Nagler's KiinstUrlexihon.
MENHADEN, economically one of the most important
fishes of the United States, known by a great number
of local names, "menhaden" and "mossbimker" being
those most generally in use. In systematic works it ap-
pears under the names of Clitpea menJuxdfn and Brcvoor-
tia tyrannus. It is allied to the European .species of shad
and pilchard, and, like the latter, approaches the coast in its
wanderings in immense shoals, which are found throughout
the year in some part of. the littoral waters between Maine
and Florida, the northern shoals retiring into deeper water
or to more southern latitudes with the approach of cold
weather. The average size of tho menhaderf is about 12
inches. Although it was long known as a palatable table-
fish, and largely used, when salted, for export to the West
Indies, and as bait for cod and mackerel, tho menhaden
fishery has been developed to its present importance only
witliin the last twenty years. A largo fleet of steamers
and sailing vessels is .engaged in it ; and a great number of
large factories have sprung into existence to extract the oil,
which is used for tanning and currying, and for adulterat-
ing other more expensive oils, and to manufacture 1 he refuse
into a very valuable guano. In the year 1877 2,426,589
gallons of oO and 55,444 tons of guano were produced.
M E N — M E N
11
^n extensive business is also carried on in converting
(Denhaden of a suitable size into " American sardines."
A very complete account of this fishery is given hy G. Brown
Soode iu "The Natural and Economic History of the American
Uenhadcn," Uniled Slates Oommunon »f Fish and Fisheries, part
r., Washington, 1879.
MENIN, a small Belgian town, in the province of West
Flanders; it is traversed by the river Lys, which there
forms the boundary between France and Belgium. The
population in 1880 was 10,200. Commercially and
iudustriaUy Menin ranks high for its size, possessing, os it
does, important manufactures of linen, oil, soap, <Sic., as
ivell as sugar refineries, breweries, and tanneries, and a
jood corn ana cattle market. Tobacco is extensively
crown in the neighbourhood, and forms one of the main
ftems of lawful trade, a good deal of Ulicit traffic also being
Miried on across the French frontier.
Mcnin does not appear to have been in any way worthy of note
antil the 14th century. Philip II. caused it to be fortified in 1578.
It was takeu by Turenno in 1668. Vanban subsequently sur-
rounded it with elaborate works, and made it one of the strongest
citadels in France ; but all its fortifications were razed in 1744.
It belonged to the Netherlands in 1816, and became part of Belgium
In 1830.
MENINGITIS (from /x^viyf, a membrane), a term in
medicine applied to inflammation afiecting the membranes
of the brain (cerebral meningitis) or spinal cord (spindl
meningitis) or both.
Of cerebral meningitis there are two varieties : — (1) that
due to the presence of tubercle in the membranes of the
brain, which gives rise to the disease known as tubercular
meningitis, or acute hydrocephalus ; and (2) simple or
acute meningitis, which may arise from various causes.
Ajnong the more common are injuries of the head, exten-
sion of discEise from contiguous parts, such as erysipelas of
the scalp or caries of the bones of the ear, exposure to
cold or to extreme heat, the presence of tumours in the
substance of the brain. It may likewise occur in the
course of fevers, rheumatism, and inflammatory affections^
and also as a result of mental overwork, sleeplessness, and
alcoholic excess. This latter variety of meningitis is less
common than the former, but it is on the whole more
amenable to treatment. The symptoms present such a
general resemblance to those already described in tubercular
meningitis that it is unnecessary to refer to them in detail
(see HvDEOCEPiLiXUs), and the treatment is essentially the
same for both.
Spinal meninf}itis, or inflammation of the membranes
investing the spinal cord, generallj' results from causes of
a similar kind to those producing cerebral meningitis, —
injuries, exposure to cold or sudden changes of tempera-
ture, diseases affecting adjacent parts such as the vertebral
column or the spinal cord itself, or extension downwards
of inflammation of the membranes of the brain. It is said
to be most common in males. As in the case of the brain,
the membranes become extremely congested ; exudation of
lymph and effusion of serum follow ; and the spinal cord
and roots of the nerves become more or less involved in
the morbid process.
The chief symptoms are fever, with severe pain in the
back or loins shooting downwards into the limbs (which
are the seat of frequent painful involuntary startings),
accompanied with a feeling of tightness round the body.
The local symptoms bear reference to the portion of the
cord the membranes of , which are involved. Thus when
the inflammation is located in the cervical portion the
muscles of the arms and chest are spasmodically contracted,
and there may be difficulty of swallowing or breathing, or
embarrassed heart's action, while when the disease is seated
»in the lower portion, the lower limbs and the bladder and
rectum are the parts affected in this way. At first there
is excited sensibility (hyperaesthesia) in the parts of the
surface of the body in relation with the portion of cord
affected. As the disease advances these symptqnis give
place to those of partial loss of power in the affected
muscles, and also partial anajsthesia. These various
phenomena may entirely pass away, and the patient after
some weeks or months recover ; or, on the other hand, they
may increase, and end in permanent paralysis.
The treatment is directed to allaying the pain and
inflammatory action by opiates. Ergot of rye is strongly
recommended by many pliysicians. The patient should
have perfect rest in the recumbent, or better still in the
prone, position. Cold applications to the spine may be of
use, while scrupulous attention to the functions of the
bladder and bowels, and to the condition of the akin with
the view of preventing bed-sores, is all-important.
Epidemic Cerebrospinal Meniiujitis. — This n.-iine, as well as
cerebrospinal fever, is applied to a dise.ise defiueJ iu tlie Nomcnela-
ture of Liseases as " a malignant epidemic fever, attended by painful
contractions of the muscles of the neck and retraction of the head.
In certain epidemics it is frequently accornpauied by a profuse pur-
puric eruption, and occasionally by cecondai-y effusions into certain
joints. Lesions of the braiu and spinal cord are found ou dissection."
This disease appears to have been first distinctly recognized in the
year 1837, when it prevailed as an epidemic in the south-west ot
France, chiefly among troops in garrison. For several years subse.
quently it existed in various other localities in France, and mostly
among soldiers. At the same time in other countries in westi^ra
and central Europe the disease was observed in epidemic outbreaks,
both among civU and military populations. In 1846 it first showed
itself in Ireland, chiefly amon;^ the inmates of workhouses in Belfast
and Dublin. Numerous outbreaks occurred also about the same
period in many parls of the United States. In more recent times
the disease has repeatedly appeared bofli in Europe and America,
but it has seldom prevailed extensively in any one tract of country,
the outbreaks affecting for the most part limited communities, such
as garrisons or camps, schools, workhouses; and prisons.
Little is known regarding the causation of this disease. All agea
seem liable to suffer, and, as regards sex, males are affected more
commonly than females. Occupation and condition of lifo appear
to exercise no influence. It nas been observed to occur most
frequently in cold seasons. The question of the contagiousness
of cerobro-spinal fever renjains still unsettled, but the weight of
authority appears to be in favour of the theory of the communica-
bility of the disease. It cannot, however, be regarded as contagious
in the same degree as some other specific fevers, such as typhus fever,
small-pox, or scarl.itina.
The following are the more prominent symptoms. After a few
(Uys of general discomfort the attack comes on sharply witli rigore,
intense headache, giddiness, and vomiting. Neuralgic pains iu
the abdomen, and pain with spasmodic contractions in the muscles
of the extremities, occur at an early stage. The headache continues
with great severity, and restlessness and delirium supervene, accom-
panied with periods of somnolence. The pains and spasms rapidly
increase, the muscles of the- neck, spine, and limbs being specially
affected. The patient's head is drawn backwards and rigidly fix6d,
the spine arched, and the anus and legs powerfully flexed, the
whole condition bearing a considerable resemblance to tetanus.
For a time there" is greatly increased sensibility of the skin, pain
being excited by the slightest contact. Tliere is more or less fever
present. About the fourth day cf the disease an eruption on tho
skin both of the face and body frequently appears, in the form
either of purpuric spots or email clear vesicles. Death may take
place in from a few hours to eight or ten days. Should the patient
survive the immediato shock of the attack, serious Complications
are apt to appear in the form of destroctivo inflammation of the
eyes or ears, inflammation with effusion into certain joints, and
paralysis of limbs ; or, again, recovery may take place after a pro-
longed convalescence. The mortality apjwars to vary in diflercnt
epidemics, iu some being as high as 80- per cent., in others only
about 20 per cent. Certain fonns of the disease are of malignant
character from the first, and very rajiidly fatal.
The changes found after death in cercbro-spinal fever are intense
inflammation of the membrane of tho brain and spinal cord, witli
effusion of serum or pus into the ventricular and arachnoid spaces.
The treatment is similar to that of other febrile conditions, but
for the special symptoms of pain, spasm, kc, opium seems to have
been foniid of eminent service, while quinine and ergot of rye are
also recommended.
MENNONTTES is a name borne by certain Christian
communities in Europe and America, denoting their
adherence to a type of doctrine of which Menno Simons
12
M E N — M E Ji
was, not indeed the originator, but the chief exponent at
the time when the anti-paedo-baptism of the congregations
in which he laboured took permanent form in opposition
to ordinary Protestantism on the one hand and to the
theocratic ideas of the ]MUnster type of anabaptism on the
other. Tlie original home of the views afterwards called
Meiinonite was in Ziirich. where, as early as 1525, Grebei
and Manz founded a community having for its most dis-
tinctive mark baptism upon confession of faitli. The chief
doctrines of these Ziirich Baptists have been already stated
in the article Baptists, vol. iii. p. 353. The main interest
of the sect lay not in dogma but in discipline. Within
the coinmnnitics evangelical life was reduced to a law of
separation from the world, and this separation — enforced
by a stringent use of excommunication and the prohibition
of marriage beyond the brotherhood— involved not only
abstinence from worldly vanities but refusal of civic duties
(the state being held to be un-Christian) — refusal to take
an oath or use the sword. In their revolt against the cor-
ruptions of the medi;eval church the Reformers neither
denied the continuity of the church as an organization nor
impugned the Christian character of the state. The new
sect did both ; and their position thus appeared so radically
subversive of the foundations of society that it is not sur-
prising, under the imperfect views of toleration then current,
that they became the objects of bitter persecution from
Protestants as well as from Catholics. But the Grebelians
had no desire, like the fanatics of Miinster, to found a new
theocracy in opposition to the anti-Christian state. They
sought only to withdraw from what their conscience con-
f'emned, content to live as strangers upon earth, and devot-
ing all their energy to preserve the purity of their own
communities. The mediaeval conception of separation from
the world as the true path of Christian perfection had
leavened all middle-cla.ss society in Europe, and prepared
many to accept separatist views of the church as soon as
they were reached by the impulse of revolt against Roman
Catholicism ; the pursuit of holiness in a society protected
by a strict discipline is an idea which experience has .shown
to have a great attraction for one class of earnest minds ;
hence, in spite of persecutions incomparably fiercer than
any of the larger Protestant bodies ever underwent, the
new doctrine and praxis rapidly spread from Switzerland
to Germany, Holland, and even to France. Each com-
munity was quite independent, united to the rest only by a
bond of love. Tltere was no sort of hierarchy, but only
" exhorters " chosen by the congregation, of whom the
most prominent were also "elders" entrusted v/ith the
administration of the sacraments — an organization so easily
kept alive or reproduced that the movement could hardly
be checked by anj' persecution short of the total annihila-
tion Vi'hich at length was actually the fate of many of the
Swiss communities. The remnants of the Swiss Mennonites
broke in 1620 into two parties, the stricter of which, the
Ammanites or Upland ilennonites, were distinguished from
the Lowland Jlennonitcs by holding that e.tcommunication
of one party dissolved marriage, and by their rejection of
buttons and the use of the razor. Their persecution lasted
till 1710; a few congregations still remain and keep
themselves quite distinct from Baptist bodies of more
modern origin. In Germany the Mennonites arc some-
what more numerous ; more important are the German
Mennonite colonies in southern Russia, brought thither ia
1783 by the empress Catherine, which in turn have recently
sent many emigrants to America. America indeed, and
especially Ponn-sylvania, .early became a refuge for the
Mennonites of Switzerland, the Palatinate, and Holland,
and is now the chief home of the body (175,000 in Uio
United States and 25,000 in Canada). Tlio oldest con-
gregation b that of Cermantown (since 1G83); the most
numerous of several divisions are the Old Mennonites, cor-
responding to the less strict of the Swiss sections.
All these communities in Europe and America are dis-
tinguished by an antique simplicity combined with antique
prejudices, by indificrenco to the interests of the greater
world, while at the same time their industry and self-con-
centration have made them generally well-to-do. Their
religious t}Tie has varied very little in the course of
centuries, as indeed is not surprising, their theology
being ascetic rather than dogmatic or speculative. The
Mennonites of Holland, on the other hand, have passed
through an interesting and progressive history.
It was in Holland and the adjoining parts 'of Low Germany that
the personal inDuence of Mcnuo Simons (1492-1.159) was mainlj
felt. He w.Ts originally a priest, and was pastor at his native place
"Witmarsum in Frie-slaud from 1531 to 1536, v/htn convictions long
ripening in his mind compelled him to resigii his cure. At this
time the anti-pxdo- baptist societies in the Low Countries were much
agitated. The vie^^is which had just before received their poUtical
deathblow at Miinster (seo Anab.1ptists) were not extiuct, and
even those who did not share them were by no means at one.
Jlenno attached himself to the Obbenites, who held that on earth
true G'hri.stiaus had no prospect bat to suffer pereecution, refused to
use the sword, and looked for no millennium on earth. Menno
became cue of their elders, and by his wanderings among the
scattered and oppressed communities, and especially hy the natural
elofjuenco and religious power of his numerous wiitings, did much
to sustain the faith of his associates, to confirm the type of their
religious life, and to prevent startling aberrations in doctrine or
discijdine. He was not an original thinker; but the love whicii
all felt for the man, and which was kept alive fo^ generations by
his writings, gave him the place which the name of Mennonites
expresses.
It may bo ascribed to the influence of Menno's wiitings that the
Dutch Mennonites, though for a time (since 1554) they broke into
fractious on questions of discipline, and especially on the effect of
excommunication upon marriage, never fell so far apart as regards
the type of their i-eligious life as to preclude the possibility of re-
union. The Waterlandcrs in North Holland, who held the least
strict doctrine of excommunication, soon moved farther in the
direction of hberality, and exchanged the name Meunonites for that
of Doopsgezindeu (Baptist persuasioii). In 3579 they refused to
contlcmn any one for opinions, even on the incarnation, which the
word of Scripture did not pronounce necessary to salvation. They
aided William the Silent with money, and from 1 'i81 to 1618 even
accepted civil office. Meantime the stricter party had undergone
various divisions, which, however, ia 1627-32 were reunited on
the basis of confessions' essentially embodying Menno's teachings.
They too had learned moderation, at le.'-st in their views of excom-
munication, and their antithesis to the state was softened since
the cessation of persecution iu 15S1, but especially since in 1672
they wore recogni^ied as citizens. On the other hand, the adofttion
of a confession had deepened the separation between them and the
liberal Doopsgezinden ; but doctrine was never the fundairieutsl
principle of tho Mennonite communities, confessionalism took no
firm root, and the two sections gradually approached, and through
a series of partial fusions became at length tinally united when the
Amsterdam congregations came together iu 1801. The pei-^uasion
declined much in nunibers in tho 18th century; since then it has
increased, and has now 127 congregations with nearly 50,000
members. Tho objection to hold civil olFice disappeared in 1795;
that to carry arms in the war of freedom against Napoleon. Baptism
on profession of faith and tho refusal of the oath, tolerance in
matters of doctrine without religious indilferenco, are tho chief
marks of the body, which in poiut of theological culture nud
general enlightenment, philanthropic zeal and social importance,
has long stood very high.
Atilhorillcs.—The best life of Memo s :r : i , C; i:ii''r"s, isa7. De Hoop
Scliclfor'3 article In nciios.l'lltt, H. f: , ■ ' ilv uno point of consc-
qiion:.^ i.T hi3 account seems to call fn i "1 i? book ;ic.>lnst John
of Leyilcn. s-ilil to luivo been publislic^l t- ■ 'i - j uncd rhc <)bbenllc!». 1«
almouc ccrtuinly spurious^ See Scpp. o ,,i.< .-.j--; ..y.: .\\np-^riit'jfn. 1. (1S7".'>
p. 128 sq. Tlio conipluicst cdlrloa of Mcnnoa »uilis b lliat In folio, ICSO. Man.v
of them aio known only In bad Dutch vcislona; Mcnno lihnscif wrote In the
"Oostcrsch" or East Sea Dialect of Low German. For the literature on the
Mennonites In gcneial, see Dj Hoop Scbeffer, on whom tho forcpoln^ sketch \*
mainly UcpcndcnL
MENSHIKOFE, Alexander D\NTL0vicn (1672-1729),
born at Moscow on the 17th of November (o.s.) 1672, was
tho son of a poor man, who employed him to sell cakes
about the streets of that city. In this humble occupation
he attracted tho attention of Lefort, one of Peter the Great's
most active co-operators, who was pleased with his spright-
liness, and took him into his service. Peter, soon afterwards
M E N — M E N
13
seeing tao youtu at JLefort'B, was also delighted with him,
and took him to be his page. Menshikoff soon became
indispensable to the czar, assisting him in his workshop,
and displaying signal bravery in the company of his master
at the siege of Azofi He formed one of the suite of Peter
durin" his travels, aud worked with him at Saardam and
Deptforo Throughout his wars with the Swedes, Men-
shikoS was the companion of the czar, and greatly distin-
guished himself For his gallantry at the battle of the
Neva, on the 7th of May (o.s.) 1703, he received the order
of St Andrew. In 1 704 he was made general, and at the
request of the czar created a prince of the Holy Koman
Empire. His house on the Vasilii-Ostroff was magnificent ;
there ambassadors were received, and banquets were given
gorgeous with gold and silver plate. Unfortunately there
is a dark side to the picture, and the favourite was guilty
of extortion to such an extent as to bring him under his
master's censure. On the death of Peter the position of
Menshikoff became very perilous ; his successes had raised
about him a host of. enemies eager for his downfall The
Goiitzins, Dolgoroukis, and all those who formed what may
be called the Old Russian party, wished to proclaim the
son of Alexis emperor. Those, however, whose aggrandize-
ment was bound up with Peter's reforms — Menshikoff,
Apraksin, Bontourlin, Goloffkin, and others — were in favour
of giving the cro\(Ti to Peter's widow, who accordingly
ascended the throne as Catherine L During her reign the
influence of Menshikoff was unbounded, and he virtually
governed the country; but the empress died in 1727,
after a reign of two years. She had made a will, no
doubt at the instigation of the favourite, to the effect
that Peter, her grandson, was to be czar under the guardian-
ship of Menshikoff, whose daughter Mary was to be married
to the youthful sovereign. Under pretence of taking care
of the young czar, Menshikoff caused him to be removed
to his house and surrounded him with his creatures. He
was now at the height of his power ; foreign ambassadors
remarked that even the great Peter himself was never
feared so much. The young czar, however, showed no
affection for Mary Menshikoff, and the girl was equally
apathetic towards her betrothed, being in, love with a
member of the family of Sapieha at the time her father
had forced her into the engagement. The Dolgoroukis
used the aversion of the j^oung prince to his Jiancee as a
means of creating dislike to the father. A chain of cvcut.'l
was gradually leading to the downfall of the favourite)
He was soon refused admittance to the summer jialace,
whither the young czar had retired. Kext he was arrested,
and so overpowered was he at his disgrace that he
had an apoplectic stroke. In vain did he addi-css Icttei-s
both /to the empetor and his sister. Shortly after, by
order of the czar, the fallen magnate de^xirtcd from
St Petersburg, but more like a nobleman retiring to his
estate than a culprit going into e.xile. The pcoplo regarded
him with dislike, and most of them rejoiced over hU fall.
On his way a courier arrived with orders to take the
czar's ring of betrothal from his daughter Mary and "ivo
her back her own, which had been worn l)y Peter H.
Menshikoff was not permitted to jiass through Moscow,
but was conducted to Oranienburg, in the government of
Eiazan, and there placed under strict surveillance. Soon
afterwards the whole family was banished to Siberia, and
arrived at Berezoff to^vards the end of 1 727. Moushikoff's
wife died on the journey, and was buried neai Kazan. On
the arrival of the prisoners they were lodged in a wooden
house, consisting of foiu- rooms. But Menshikoff did not
long endure the horroi-s of exile in this inclemout region.
According to Mannstein, he died (Xovember 13, o.s.,
1729) of an apoplectic stroke, because there was no one
at Berezoff, as he himself remarked, who understood how
to open a vein. The young cz.ir ordered the release from
exile of the two remaining children of Menshikoff, — his
daughter Mary had died at Berezoff in the same year
as her father, — ^and restored some of their property to
them.
MENSHIKOFF, Alexa>t)er Sergeievich ( 1 787-1 869),
great-grandson of Peter's favourite, bom in 1787, entered
the Russian service as attache to the embassy at Vienna. He
accompanied the emperor Alexander throughout his cam-
paigns against Napoleon, and attained the rank of general,
but retired from active service in 1823. He then devoted
himself to naval matters, and put tire Russian marine,
which had fallen into decay during the reign of Alexander,
on an efficient footing. On the outbreak of the Crimean
War he was appointed commander-in-chief, and suffered a
severe defeat at the Alma. On the death of the emperot
Nicholas in 1855 he was recalled, ostensibly on account
of failing health. He died in 1869.
MENSUKATION
"VrENSURATION, or the art of measuring, involves
ijj. the construction of measures, the methods of using
them, and the investigation of rules by which magnitudes
which it may be difficult or impossible to measure directly
are calculated from the ascertained value of some associated
magnitude. It is usiial, however, to employ the term
mensuration in the last of these senses; and we may
therefore define it to be that department of mathematical
science by which the various dimensions of bodies are
calculated from the simplest possible measurements.
The determination of the lengths and directions of
straight lines, including what are familiarly knowTv.as
problems in heights and distances, generally depends on
the solution of triangles, and will be discussed in the
articles Tkigonometey and Scteveying. The remaining
iwrtiona of the subject are the determinations of the
lengths of curves, the areas of plane or other figures, and
the volumes and surfaces of solids ; and it is of mensura-
^on as thus restricted that the present article will discuss
some of the more important problems.
§ 1. Uniti of Length, Area, and Volume. — In measuring
any magnitude we select some standard or " nni' " 'o -nea-
sure by. Thus in measuring length we take for unit an
inch, a foot, or a yard. From the unit of length we derive
the imits of area and volume. Thus we define the unit of
area to be the area of the square described upon the unit
of length, and the unit of volume to be the volume of the
cube whose edge is the unit of length or whose side is the
unit of area. For example, if an inch be taken as the unit
of length, the square whose side is 1 inch is the unit of
area, and the cube whose edge is 1 inch is the unit of
volume. The length of a line, the area of a surface, and
the volume of a solid are then expressed by the numbers,
whole or fractional, of units of length, area, and volume
which they respectively contain. Hence, if I denote the
linear unit, the length of a line which contains a units is al,
or simply a since / is unity ; similarly the area of a surface
which contains b units of area is bm, or simply b, where
m is the unit of area.
§ 2. Commensurable and Incommensurable Magnitudes. —
When two magnitudes have a common measure, that is,
when another magnitude can be found which is contained
in each an exact number of times, they are said to be
" cf>'".mensurable." Thus « 'Jne 4 J ai'd another 3J inches
14
MENSURATION
long are commensurable ; for, if J inch be taken as unit of
length, tlie former contains the unit nine times and the
Utter seven times. If no common measure can be found,
jhe two magnitudes are said to be "incommensurable."
For instance, 1 and ■Ji have no common measure ; for
v/2 = l'4142 ... an interminable decimal, and hence no
unit, however small, can be found which will be contained
in each an exact number of times. If, however, we take
^/2 = l•4, the error \vill be less than jV; '^ s/S- 1-414,
the error will be less than xviyist ^'^- Hence, by taking a
sufficient number of figures, we can find a fraction which
will differ from \/2 by less than any assignable quantity,
and therefore we can always find two commensurable
magnitudes that will represent two incommensurable ones
to any degree of accuracy we please. In what follows we
need therefore only consider commensurable lines.
§ 3. Area of a Bectangle. — Let the side AB (fig. 1) con-
tain a units and the side BC b units of length. If we
divide AB into a equal parts, j^ ^
each equal to the unit of length,
and similarly BC into 6 equal
parts, and if through the points
of 'division we draw lines
parallel to the sides of the
rectangle, these lines will di-
vide the rectangle into a series
of rectangles, each of which is
the unit of area, since each is
a square whose sides are of
unit length. As we have a rows of these rectangles, and
h in each row, the whole rnunber of rectangles wUl be ab.
Therefore
area of ABCD— o6 onits of area
—aft.
'•ig. 1.
SEono:T
PART I.— PLANE FIGIIRES.
-Plane Fioitres contained bt Steaioht Lines.
A. The Rectangle.
§ i. Let ABCD (fig. 2) be a rectangle,
BC-DA = i, AC-c, and the angle A
BAG — a ; it is required to find its area.
Since a rectangle is completely de-
termined when two independent data,
one of \7liich at least is a length, are
given connecting its parts, we can de-
termine its area in the following cases.
(o) IVhe/i its length a and its breadth
b are given. — It has already been proved
(§ 8) that Fig- 2-
area of ABCD- o5;
or the area of a rectangle is equal to its length multiplied by its
"breadth. ■
Example. — lift a — 12 feet 6 inches and J — 9 inches, then
area of ABCD-12-5x -rS-D'STS square feet
If we make use of logarithms in the above, calculation we have
log area — logo + logfi .
loga-logl2-5 -1-0969100
log 6 -log -75-1-8750613
therefore logarea- -9719713;
hence area.— 9-375.
{(3) When a side a and the diagonal a an givm. — By Eodid
i. 47 wo have
f-e'-a', or t-Vc'-o',
therefore area of ABCD - a!i - as/er - a' ;
or logarca-loga + 41og((; + a)-l-Jlog(e-(«).
Example.— Let a-238 and c-456, then
loga- log238-2-3765770
41og(i; -Ha) -}log694- 1-4206797
41og(g-a)-ilog218- 1-1 692282
therefore log area -4 -9664849 ;
hence ' area -^2573 -I .
iy) When a tide a and a iU inelinaiion to the diagonal are ffUMW
-Since '
— — tan a
3 tana
and therefore area of ABCD -ab- o'.tan r. ;
or logarea-21oga-HLtana- 10.
Example.— T^\, o-36 and a-32° 26' 15", then
21oga-21og36- 3-1126050
Ltana-Ltan32° 26' 15"- 9-8028622
therefore log area- 12-n54672- 10-2-8154672;
hence area -823 -127.
(5) WTicn the diagonal c
sides are given. — We have
nd a its inrlinnHon to either of the
o — ccosa, and ft — esinc,
therefore area of ABCD-aJ-c'sinaoo8o-ic'ain2o:
or 2area — c-Biu2o,
and hence log2area-21ogi;-i-Lsiu2a-10.
§ 6. A square being a rectangle whose ^des are equal, we can at
once determine its area. When one datum, which must be a
length, is given the square is completely determined, and bene*
n e have only two caaes to consider.
(a) When tlie side is given.— Ftom § 4, a, we have at once
. » area of square — aft- a X a — a*.
(B) When the diagonal c is given.— fvoxn § 4, p. we have
a* -t- a' — c^, or a' — Jc* ;
hence area of aquare- n' — Jc', or 2area — c*;
and therefore log 2 area -2 log e.
B. Might-angled Triaugles.
§ 6. The diagonal of every rectangle divides it into two eqniva*
lent right-angled triangles (Eucl. i. 34), and hence the area of the
right-angled triangle ABC (fig. 2) is equal to half the area of th«
corresponding rectangle ABCD.
r Ge^urally.
e six elements to be CO!isider«d,
C. Triangh
% 7. In every triangle there a
namely, the three sides and the
three angles. If any three of
these six be given, provided one
is a length, iho triangle is com-
pletely determined, and hence
Its area can be found.
§ 8. Length of Perpcndictilars
of a Triangle.— In the triangle
ABC (fig. 3) let BC-er, CA-6,
AB = c, AD the perpendicular
from A on BC-A, BD-a;,
and CD-;;.
*'"ce BDA and CDA are right angles, ,wo have
c' — a;'-H/i', and ft'-j('-h7i',
and therefore
ft3 _ (J - 3/2 - a:» - (y -l- a-Xy - s) - 0(1/ - r) ;
whence y--x—
But y + 1 — a, and, by solving these equations, we obtain
ft'-Hn'-c»
Fig. 3.
Again
,,.ft,.;^-ft._(^i±^')'
(2aft)'-(i.'-Ha'-c')'
(g-t-ft-t-c)(ft-l-i:-a)(<;-l-g-ft)(o-Hft-c)
4a=
henc4- .h~ — \/(a-Vh + c)(i-i-c-a)(c + a-bta-k^h-r).
2a
Now let a + t-t-e-is, then b + c-a-2(,s- a) , e + a-b — iit-b),
and n + J-c-2(s-c)-
Therefore, on substituting and reducing, we obtain
h--\fs{s-a){s-b){s-e).
Similarly the parpendiculars from B and Qjjn fho opposite side*
arc respectively
-^V«(s-a)(»-ft)(«-<i), and -^•v'»(«-;ol(»-ftl(«-.el.
§ 0. We now proceed to invcsligato'forulnlf^ lor tno antj'of a
triangh) in tlfe following Snportant cases. ■
'a) "•''■•™ the base, » and the altitude h life Jieerf.— MuTl* •
MENSURATION
15
triaogls is eqnel to half a rectangle of the same base and altitdde,
we have at once
aieaABC — ian.
Example. — IJet o— 40 chains and A=14'52 chains, then
area — ix40xl4'62 = 290'4 scjuare chains.
(3) Whm two tides a and c and the included angle B or« giv&a,—
Trom fig. S — — sinB, and therefore A=C8inB ;
hence area— JitA—Jac sin B ;
or log2area=loga + logi; + L9inB-10.
Example. — Let a— 40, c=30, and B-^SO", then
area = Jacsin B = J x 40 x 30 x i = 300.
(7) JFAct the three sides a, b, c are given. — From § 8
A-| V«(»-o)(«-6)Ca-c),
and therefore
area-ioA-Jax— V«(s-a)(»-i)(s-c)-Vs(«-a)(s-6)(»-(;) ;
or logarea.=-J{Iog« + Iog(s-ii) + log(s-i) + log(«-(!)}.
Since 2j— a+J+c, we have
area of triangle - }V2(a=6» + J^c^ + c'a") - ((»*+6«+'<:*) .
Examvlel. — Leta-13, i-14, aiidc-lS, then
«-i(13 + 14 + lB)-21, »-a-21-13 = 8,
(-6-21-14-7, ands-c-21-15->6;
therefors area = V2fx8x7x6- 84.
JSoompfa 2.— Let 0-255, 6-238, andc-221, then
logs-log357- 2-5526682
log(s-a)-logl02- 2-0086002
log{j-6)-logll9= 2-0755470
log(s-c)-logl36- 2-1335389
therefore log area - i(8 '7703543) = -l -3851 771 ;
hence area — 24276.
(t) TfTien any two angles 6 mid C and the adjaeent tide a are
given. — Since
c sinC asinC
a sinA ' sinA '
and therefore (by ff)
area - iocsin B - "'"".^""P , where A - ISO" - (6 + 0) ,
or log2area=21ogo + L8inB + LRinC + LcosecA-3D.
Since all the angles of a triangle are given when any two are
given, we can find the area of a triangle when any two angles and
any one side are given. Thus, when A, B, and c are given, wo know
C also, and the problem reduces to a case of the preceding.
(c) When the three medians a, 0, y are given. — If a, 6, c be the
three sides of a triangle, and o, ft 7 the three medians, i.e., the
lines drawn from the angles to the middle points of the opposite
sides, then by veil-known geometrical propositions we have
4(a'" + 18= + 7^) = 3{a' + 63 + c2) ,
16(o=/3» -, 3V + Vo"-) - 9(a26= + 6V + c=a2) ,
and 16(o*+J3*-+7«)-9(rt« + 6< + <r«).
Now (§ 9, 7) _
area of triangle -}V2((i='d" + 6'c= + i;W
therefore
-ja' + h' + c'),
■ J V-2(a=e' + ^V -t- yo') - (o« + /3« + V) .
D. Parallelograrns.
§ 10. The opposite sides and angles of a parallelogram being
equal, three independent
data, one of which at least
is a length, are necessary and
sofiicient to determine it
comjiletely. .
In the parallelogram ABCD
(fig. 4) let BC = DA-a,
AB-CD-6, AC-c,AE = A, B
the angle ABC -a and -. .
AOp-ft ^'S- ^•
Since the diagonal AC divides the paral'o'ogram into two eqni-
valent triangles, we obtain
(o) area of ABCD = 2 area of triangle ABC
-2x4axA(§9, a)-oA;
{$) areaof ABCD = 2areaAB0 = 2xia6sino{§9, j8)-o6sinoi
or logarea=loga + log6+Lsino-10 ;
(7) area of ABCD-2 area ABC-2(AB0"+CB0)
•■2{iB0.A0sinA0B + JBO.COsinCOB} -2{iBO.AC3in/3}
— JBD. AC sin 8 — Joisin IS ,
ot log2Brea-logc + logd + LBin/3-10.
§ 11. If the parallelogram be equiangtUar (a rectangle), c<=d,
and area -J«»8inj8. If it be equilateral (a rhombus), p-90°, and
area — Jcrf. If it bo both eguiatigular and eguilatcral (a square),
c-d and fl-90°, and aiea - Jc" as before (§ 6, 0).
E. Trapesiunis.
§ 12. To determine a trapezium completely four data ai'e neces-
sary and sufficient.
In the trapezium ABCD (fig. B)letBC=a,CD-J,i)A-=(;,AB-(<,
Fig. 6.
and AE perpendicular to BC = A, and draw AF parallel to CD,
then
(o) area ABCD = area ABC + area ADO
'^\ah + \ch
— J(a + c)A;
or the area is e^ual to half the sum of the pai-allel sides multiplied
by the perpendicular between them.
Again, area of ABF - ^BFx AE (§ 9. a)-^{a-c)h,
also area of ABr= V«(s- AB)(«- BF)(s-FA),
where 2« = AB-(-BF + FA ;
hence ft-^^V«(s - AB)(s - BF)(s - FA), therefore
iff) area of ABCD - 4(a + o)k='^^^\/ s(3 - AB)(» - BF)(5 - FA)
■■ J^^'V(-a+6+i!+(i3(o.+ 6-(!-d)(a+6-c+d)(a-J-(!+d) ,
since AB-rf, BF-(t-c, and FA-CD-6.
Thus we can find the area of a ti-apezium in terms of its sides.
§ 18. If c — 0, ABCD becomes a triangle, and its area
-jV(-o-l-6-l-rf)(a + 6-d)(a + 6 + d)(o-i + d).
Again, if c-os, then also b=d, and ABCD becomes a parallelo-
gram, and its area takes the indeterminate form—, as it should do,
since four sides do not completely determine a parallelogram.
F. Quadrilaterals Generally.
§ 14. A quadrilateral is completely determined when five inde-
pendent data arc given. "We consider the following cases.
(a) When any diagonal and the perpendiculars on it from, the
opposite vertices are given.
The quadrilateral ABCD (fig. 6) =ABD + BCD
-iBD.AK + JBD.CF
-JBD(AE + CF)j
or the area is equal to half the product of the diagonal and the
sum of the perpendiculars. .
If the diagonal BD fall B^
without' the ficrure, as in tho
concave quadrilateral ABCD
(fig. 7), then it is clear that
area ABCD = JBD(AE - CF).
(ff) When the diagonals and
tlieir included angle ate
given. — In the quadrilateral
ABCD (fig. 8, p. 16) let BD-h, AC-=*, and angle DEA-
ABCD -ABD+ BCD
= iBD.AEsina + iBD.CEsino(§ 10. 7)
-P(AE-l-CE)sina
— iA^sina ;-
or the area is equal to the product of the diagonals and tiie sine ot
their contained angle. -
Tho same result holds -
when one of the dia-
gonals falls without tho
quadrilateral, as in fig.
7, as the reader can easily
verify.
(7) JFhen the four
sides and the angle be-
tween the diagonals
given. — If a, b, e, d be ,ij„ -
th? sides and a the angle
between the diagonals it can easily be shown that
^a of quadxilatoral-J(a'- V'-t-c'-'P^tauo.
Fig. 6.
, then
16
MENSURATION
(>) fFlien Iht four tida art given and Die oppotiU angla are
tuml*nuniary.—la fig. 8 let AB-o BC-4, CD-c, DA-d,
AC -A, angle ABC-o, angle j^^
GDA-i5, and let o + fl-180*.
then
areaof ABCD - ABC + ADC
— iabaina + l^cdemp.
But
lin^- Bin (180*- a) — sis a,
therefore
areaof ABCD- i(ai + c<j) sin a. 0
This gives us the area of the ^'8- 8.
<luadriUteraI in terms of the four sides and one angle.
Again we have
a' + lr-2alcoaa~h'-c' + d'-2cdcoa0-c' + £' + 2cdci>sa
a' + lfi-e'-d' ,,
- , and hence
1 +cosa
', and
therefore ^w-«— „, ,
2{ab + cd)
Ja + b + c-d){a + b-e + d)
2(a6 + a!)
1 cos i' + d + a-b){e + d-a + b)
"" 2(a6 + oi)
From this we ohtain
ein'a- (1 + cosaXl -coso)
{b + c + d- aye -■■I't- a-b){d + a + h-c){a + b+e-d)
Mab + cd)'
N(iw let a + b + c + d-Zi,
t£c». J(ai + erf) sin a — V(» - a){s - 6)(a - c){j - d) ;
{horefore nrea of ABCD - \^(s - a){s - 6)(5 - c){s - d) ,
or log area — i{lop(s-o) + log(s-i) + log(3-<;) + log(s -a!)) .
If rf = 0, the quadrilateral becomes a triangle, and its area is
■>/(» - o)(s - i)(» - c)s as before. In extracting the square root of
sin a we take the positive sign, since the angle a is less than two
right angles.
G. Regular Polygons.
§ 16. Since a regular polygon is both equilateral and equiangular,
a circle can bo inscribed vrithin it and also described about it, and
thus the n straight lines drawn
from the common centre of the
two circles to the n vertices of the
polygon divide it into n triangles
equal in every respect. Therefore
the area of the polygon is equal to n
times the area of any one of these
triangles.
§ 16. Radius of Inscribed and
Circumscribed Circles.- — Let AJ5 (fig.
9)=- a be a side of a regular polygon
of u sides ; let C be the centre of
the inscribed and circumscribed
circles, CD — r the radius of the
former, and CE — R* the radius of the
latter. The angle ACB
right angles, that is
Fig. 0.
evidently equal to the nth part of four
A.CB.
aeo"
and ACD-
AD =
. CD tan ACD ~r tan
iACB_i^.
180*
AD---ACuiiACD = Rsin— ;
= (xx 4cot-
and Jl^dxicosec .
§ 17. Perimeter of Polygon. — The perimetar of the, polygon of
. , . . „ 1 180° „ D • 180°
» Bides IS na, x.e., 2nrtan , or 2nRsm .
n n
From this it fdllows that tho perimeters of the inscribed and circum-
scribed regular polygons of n sides of a circle of radius r are
. 180° , „ , 180° .. ,
2nrsm and 2nrtan respectively.
§ 18.' Area of Polygon.
(a) In terms of r.— The area of polygon
-7iACB-nAD.CD-nxr»tan— - .
360°
(fl) In Urmt of K—rbe triangle ACB
— JAC . CBsin ACB- JR'sin'
and therefore area of polygon — JnE^sin .
(7) In terms of a. — The triangle ACB
'i.n /-rr> o o t .180° a" ^180*
-iAB.CD--i5- xr— — X Jacot ——cot
and therefore area of polygon — a^ x col ■^.-
j4arca-logn + Lcot?^ + 21ogi
-10.
Fro-ii a and fi it follows that tho areas of the inscribed and ciicam-
scribed regular- polygons of n sides of a circle c! radius r ar«
inr^sin*" and Tir^taji respectively.
18, y) for the area of a polyguu, the
§19. In the formula
has a definite value for every valuo of n, and henoe,
factor
if we find its value once for all for a large number of values of n,
and tabulate the results, we can find the area of a regular polygoit
of 7! sides by multiplying the sausre of its side by the ai>propnat«
tabular value.
Again, if a — 1 we have
180° ._j _ , 180°
■icoti
and n — i c
and thus we obtain in a similar manner the radius of the inscribed
and circumscribed circles by multiplying the side by the appro-
ISO*' 180*
priate tabular value of Jcot and Jcoseo respectively.
§ 20. The following table icnrains the values of —cot — - and
in
180° 180*
their logarithms, and the values of J cot ■ and Icosec for all
n ' n
values of n from 3 to 12.
"
"cotlfl
Loff&iithma.
Jeotl^
,e«.c^
3
0-4330127
1-6305006
0-28S67
■677M
4
10000000
OOOOOOOO
O-5OO00
•70710
S
1-7204774
0-2366490
C-68819
-85065
<
2-0980762
0-4146519
O8C60J
1-0000
7
S-6339124
0-5005746
1-0383
1-1523
8
4-S284271
0-6390568
1-2071
l-SOtt
9
61818212
0-7911166
1-3737
1K13
10
7-6942088
0-6861040
1-»3S8
1-6180
11
93650407
09715375
1-7028
17747
12
11-1961M4
1-0490688
1-8660
1-9318
Let A denote the area of a polygon of n sides and A' tho cor-
responding tabular value of — cot , then
A-a=A',
or logA — 21ogiz-)-logA'.
U.— Length of the Radius of tU Inscribed, Escritea,jl7ut
Circumscribed Circles qf a Triangle.
§ 21. [ai Radius of
Inscribed Circle. — LctO »
(fig. 10) be the centre of "*
the circle Inscribed in
tho triangle ABC and
touching the sides in D,
E, and F. Join OA,
OB, and OC. The
angles -at D, E, F are
right angles (Eucl. iii.
18). Let BC-a, CA
-6, AB-c, and CD
-OE-OF-r. B
Now ABC-BOC p. jQ
■f COA-t-AOB *'^- '"
• iar + ibr + icr-i{a + b + c)r-rs
areaof ABC s/s{s-a){s-b){s-c)
rlience r — — • —
s s
(0) Radius of Escribed Circles.— het OD-OE-0/-ra, then
ABC - ACQ -I- ABO - BOC
- i^Ta ■^ irra - Jar. -i(4-!-<r - a)r,-rj,s-a) ,
and
Cimikrly
area of ABC V»(« - a)(J - ^)(^ -c) /.■is-b){s-e) ^
n-y^^^^^-^^-s/^^'^--
M E N S U R A T I O 1.'
17
{yYSadiua of Oircumscribed OircU.—'Let AD (fig. 12)-p the
perpendicular from A oa the eide BC, and AE-2R the diameter
Fig. 11. Fig. 12.
«f the circle, then (Eucl. vi. C) we have
2'Rxp = bxc,
therefore SRxap = abc.
Now ap = 2A, where A denotes the area of ABC ;
abc abc
hence
R=^ = -
Ws{s-'a)(s-b){s-c)
lie. — Let a = 13, b = li, and<;=15: then r will he found
to be 4, v. lOi, n 12, r, 14, aud E 8J.
Section II.— Plane Fiocres contained by Ccilved Lines.
A. The Circle.
§ 22. Circxtmfenrwe of a Circle. — If we inscribe in any circle a
regular polygon of n sides, and also circumscribe a regular polygon
of the same number of sides, it is clear that the perimeter of the
circle is intermediate between the perimeters of the inscribed and
circumscribed polygons, and that the difference between the peri-
meters of the inscribed and circumscribed polygons can be made as
small as we please by sufficiently increasing n. A similar state-
meut holds with reference to the areas of the circle and the in-
Bcribed and circumscribed polygon;. With the above assumptions
it is easily proved that the circumference of acircle bears a constant
ratio to its diameter. Hence we have
Circumference = C = constant x radius = constant x r.
It is usual to denote this constant by 2ir, and therefore
C = 2jrt'=ffrf, where d is the diameter of the circle.
§ 23. Numerical Value of ir. — The constant ir being, as can be
easily proved, an interminable decimal, we can only approximate
to its value, but this we can do to any degree of accuracy we please.
If s and <r denote respectively a side of the inscribed and circum-
scribed polygons of n sides, and s' and t/ a side of the inscribed
and circumscribed polygons of 2» sides, it can easily be shown that
<«^ '=V^=pf. (B)^=2r \ ~V?qiip j ,
(7) </ — , — — ,
where r is the radius of the circle.
If we take r= 4 we find, by means of these formulae, and by
assuming the value of s when « = 6, that the perimeter of inscribed
polyfjon of 96 sides=3140 .... , and the perimeter of circum-
scribed polygon of 96 sides=3'142. ...
; From this we learn that the circumference of the circle, in this
case IT, is greater than 3'140 .-. . . and less than3°142. • • . ,
and therefore as far as the second place of decimals
ir = 3'14.
By taking greater, and greater values of n we obtain closer and
closer approximations to ir.
• 1 The preceding method for approximating to the value of ir is the
simplest afforded by elementary geometry, and is also the oldest ;
but better and more rapid methods are furnished by the higher
mathematics. The calculation of ir has been carried to 707 places
of decimals, the following being the first 20 figures in the result: —
3-141592653589-9323846.
iTor all practical purposes it is sufilcient to take
.=3-14159 or=|||.
§ 24. The following table contains the functions of » that are of
Imost frequent occurrence in mensuration : —
■ Nomber.
Loearithm.
Nambcr.
Logarftbm,
w ■
3H15027
0-4I)7M99
n'
9-8096044
0-9942097
2n-
■ C'28318,53
0-7981799
_1_
Ati
12'5053706
1-0992099
0-0168869
2-227M90
1-5707903
01961199
l-0471!)76
0-78S39S2
00200286
I -8950899
Vt
1-77245S9
0-2485760
V
0'623.Me8
1-7189986
V-
1-4645919
0-1657168
w
0 -3920901
1-6940599
t
0-2617994
I-4179GS8
*
0-5641696
1-7514351
4-1887902
O-C220868
180
0'0I74!33
2-2118774
Vt
1-1283792
0'05345S1
4
0-3183099
T-5028501
Wi
0-2820948
1-4603051
1-2732395
0-1049101
^~
1-2407010
0-0936C71
tir
0-0795776
5-9007901
V4.r
0-.6203505
1-792S371
67-2957795
1-7681226
log.,r
1-1447299
00587030
Fig. 13.
§25. Units of Angular Measurement. — In measm-ing lines we
select some line of constant length as the standard or unit ; simi-
larly in measuring angles we require to take some angle of constant
magnitude as unit angle. The right
angle is by its nature the simplest unit
angle, but, for convenience, we take the
■sVth part of a right angle for unit, and
call it a degree, which is subdivided
into sixty equal parts called minutes,
and these again into sixty equal parts
called seconds. For theoretical purposes
we define the unit angle to be tlie angle
subtended at the centre of a circle by an
are equal to tlie radius. This angle we
call a "radian." In many treatises the
radian measure of an angle is called
the circular measure.
§ 26. The radian is a constant angle. — Let OA (fig. 13)=arc AB
= r, then AOB=radian, and let AOD=90°j then
arc AD = ix2-irr= i-irr ;
and, since angles at the centre of a circle are proportional to the
arcs on which they stand ( Eucl. vi. 33),
number of degrees in radian AOB_ AB r _2_
number of degrees in AOD AD iwr ir '
therefore number of degrees in radian
= 90° X — = 57''- 2957796 = constant.
n
§ 27. Number of Radians in any Angle.— het AOC (fig. 13) ho
any angle, AOB the radian, and AC=s ; then
nnmber of radians in AOC AC _ _«_ .
one radian AB r
therefore number of radians in AOC=
r
If AOC=90°, then s=iirr, and number of radiana=iir ; there are
thus IT radians in two and 2ir in four right angles.
When r=l we have number of radians = s, and hence in some
treatises for the number of radians in an angle we find the length
of the arc given.
§ 28. To transfer from degrees to radians and conversehj. — Let a>
denote the number of degrees in an angle, and 0 the number of
radians in the same, then, since ^5773 =-2 >
180„
180°
§ 29. The following table contains the valnes of 0 for valncs of
a; up to 180°, and also for minutes and seconds.
•s
s
S
s
Radi-
1
Radian.
£
RadluQ.
£
Radian,
Radian.
a
an.
Q
0
a
-0
s
-000
1
•0174533
61
I •0e4C508
121
2-1118484
1
002909
1
0048
2
-0349066
(17
i-os2ion
li'l!
2-1293017
2
005818
2
0097
3
■0523599
03
1-0995674
123
2-I4C76.50
3
008727
4
•0C.98132
04
I -1170107
124
2 1042083
4
011030
4
0194
5
■0872065
or.
1-1344610
r.>5
2-1810610
6
014544
6
6
•1047198
60
1-1119173
120
2-1991149
6
017463
7
■12-.'1730
07
1-1093700
1-17
2-2105682
7
020362
7
fl
■1396263
08
1^18C8239
12s
2-2310214
H
023271
H
0388
9
•1570790
69
I ■201-2772
129
2-2514717
9
020180
9
0436
10
■1745329
70
I -2217305
1311
2-2659280
10
029089
0485
20
80
1-39021134
140
2-4434010
20
058178
20
0970
90
1 -5707903
1.-.0
2-CI79939
30
087206
30
40
■C98I317
100
1 -74.'.329:l
169
2-792.'i2e8
40
116355
40
19-19
60
•8720646
no
1 -9198622
170
2-9070.',97
60
145444
60
60
I^0471976
120
2-0943951
180
3-1415927
00
174533
60
18
MENSURATION
Aa an oxamplo of the nse of this tabic we proceed to find the
valuo of 0 when a=ti3'' 45' 17" '8.
■Whcn.T=68° 9 = 1-1868239,
a = 40' «= 0110355,
a;= 5' «= -0014514,
a;- 10" e= -0000485,
x= T e= -0000339,
and when a: = 0'-89= -0000039,
therefore when ar=G8° 45' 17" '8 0=1-2000001 .
§ 30. Combining the results of §§ 27 and 28 wo obtaii
, , . s , 180 s .
(a) e= — , anda; = . — J
r ir J-
(fl) , = 4=11.0. A;
d T! X
{y) » = .(,= ^^.«.
'§31. Lemglh of Arcs of Circles.— The following are the more im-
(lortant cases; —
I (a) In terms of (he chord of the arc and the radius of the circle. —
I,8t AB (fig. 14) = 2c, AC = r, and AEB = s, then
AD = JAB=c = rsiniC, whence C is known, and therefore
the arc s is found (§ 30, 7).
^ (/8) In terms of (he height of the arc and the radius of the circle. —
Xot I)E=A=height of arc, then '
CD = CE-DE=j--fi,'
ir, CD r-h
and cos4C=--:-= ,
AC «•
whence 0 is found, and therefore 9
Fig. 14. Fig. 16.
S 32. Buygens's Approximation to the Length of a Circular Arc. —
Lot AB (fig. 15) =p be the chord of the arc AEB, and AE = EB=-j
that of half the arc, then the arc AEB = J (89 - p) approximately.
I For, let r denote the radius, s the arc AEB, and 20 the angle
ACB, then 6=^. Again, AB=2)=2AD=2»-sine=2r8in
2r '
and similarly g= 2r sin — .
Now smS^d-
therefor p=2.- j ^.^^(^^^^(i-y - &C j
2. 3. 4. 5. 16. r*
Sinularly 8, = 16. j A^-i|(^)V^(i^J - &c.
2.3. 4.r= 2. 3 . '.
Hence, neglecting powers of — be-
yond the fourth, wo obtain
approximately.
In practice it is sometimes more
convenient to use the enuiyalent
form
s=25 + 5(2g-y).
§33. Area of Sector of a Circle.—
Let the sector be CAB (fig. 16).
Divide the arc AB into n equal parts,
and draw the chords of these. Let P denote the perimeter of the
Uroken lino AB, A tho area of tho polygon AOB, and p the alti-
I'ig. 16.
tudc of any one of the n equal triangles of which this polygon ^
made up.
Now in tho limit, when n is indefinitely increased, P beco-r^s
tho arc AB=s, a result which we symbolize thus —
Jj P=arcAB=s.
Similarly
^=radiu3=r.
Again, the area of the sector is equal to the area of the polygn*
when the broken line AB becomes tho arc AB, that is,
sector = L„=„ A = L„=„ J J"< P ■= J L„_„P X L„=„ P •
= !,rs .
§ 34. Let S denote the area of a sector of a circle, then, by ueana
of tho above result and § 27, we hava
(a) S = l«-,
(6) S = irfl.r=ir=ff.
§ 35. "We proceed to find the area of a sector of a circle in thsfol-
lowing additional cases :—
(a) IVhen the chord of the sector and the radiits of the cirile ar*
given.— In fig. 14 let AB = 2i;, and let AC = »-, then we have
ACB AD c .
sin — ,— =
AC
whence ACB and therefore 0 is known, and S can be found hy % 34.
ACB has two values, the smaller one giving the area of th.; m'.nor,
and the larger that of the major conjugate sector.
(B) IVhcn tlie chord and height of the chord are giwn. — Lot
DE (fig. 14) -h and AB = '2c, then
AC2=j-2 = AD=+DC2 = (;'+(r-A)^, whence
xx=*LJi — , and therefore by previous case the aroa can be found,
(7) Wlien the chord and angle suhlended at the centre are given.
—Let AB (fig. 14) =20 and ACB = 0, then
c . ACB c -
— = sm — ;;— , or r = -: — 5-5 ,
r 2 sm^S
therefore area of sector = Jr-* = J ( ^-i_ ) x 5 .
\smi»/
§ 36. Area of a Circle. — The circle being a sector whose arc is tha
whole cii'cumfercnce we obtain at once
area of circle ■=4rxa = ^rx 2«- = irr'.
An independent proof of this proposition might be given by
means of the inscribed and circumscribed polygons, and from th»
area of a circle the area of a sector can be deduced. The infini-
tesimal calculus aflTords a simple and elegant proof (see § 44).
§ 37. If A denote tho area, r tho radius, d = 2r tho diameter, and
C the circumference of a circle, we have
(c.) A-nr-,
(^) A-Jx2itrxr = 40r,
inV C=
(7) ^-TT-ii'
ir4r' ird?
(8) K^"^-^.
■Wbence we see that the area of a circle is obtained by multiplying
(a) the square of its radius by x = 3-14159,
(/3) the radius by half the circumference,
(y) tho square of the circumference by — = -07967 ,
(8) the square of the diameter by Jir = -78539 .
§ 38. Again, from the above formuh-e we deduca
(a) r— ^ A- -5641896 x A,
Vtt
(/3) d ==A = l-1283792xA,
Vir_
(7) <!-2v'ffA-3-5449077xA,
thus obtaining radius, diameter, and circumference from area.
§ 39. Area of a Circular BiJig. — Let r and r^ denote the radii of
the outer and inner circles respect-
ively (fig. 17), then the area of the
space between them
- irr^ - irrj = ir(r ^ ri)(r - r,, .
Tho circles need not bo concentric,
and tho reader should note that tlio
area of tho ring is equal to tho area
01 an ellipse whoso major and minor
axes arc r + r^ and r- rj (see § 51).
§ 40. Area of the Sector of nn
Annulus. — Let angle ACB — fi in fig.
17, then the area of ABED
-sector ACB - sector DCE
-ir-e-ir^S,
.= i«(r+r,)(r-r,).
Fig. 17.
MENSURATION
19
igajn, letAE=?, DE=Ju andCA-CD=r-r, = ;i, then
r--3- ana 'j^-g- i therefore
r+r,=-g-(J+Z,), and
area of 8ector-.3S(r+r,j(r-r,)=i9 (l^y=ih{l+l,).
§41. Area (if a Segment of a Circle. — (a) IFTien the radius and tJu
angle subimdcd at the centre an given.— la fig. 14, let AEiJ be a
eegment of a circle, then its area
= sector AC B - triangle ACB.
= 4r'e-Jr=sinfl(§§9, 34)
= ir'^C - sin 6) .
If the segment be greater than a semicircle siufi is oegatiTB and
the formula becomes
ir'(,e + sme)
ts is also geometrically evident.
We might in a similar manner find the area of a segmcLt of a circle
(fl) when the chord and radius are given,
(7) when the chord and its height are given,
(!) when the radius and height of the chord are given,
(e) when the chord and angle subtended by the chord are given.
In all these cases the method of proceeding is obvious, a segment
beiag the (kfTerence between a sector and a triangle.
§ 42. Area of a iiin*.— Let ADB and ACB (fig. lo/ oe two seg-
ments of circles, then the area of
the Inne ADBC
—segment ADB - segment ACB.
Hence if we so choose our data that
we can determine the areas of the
two segments we have ouly to take
their difference to fiad the area of
the lune.
5 43. Area oj a Circjuar /ion». —
Let AB and CD (fig. 19) be two
parallel chords, then the area of the zone ABCD
=cbcl8 - segment AHB - semient DFC ;
or = segment AED + trapezium ABCD + segment BGO
— 2 segment AED + trapezium ABCD.
§ 44. The iNFiNrrEsiiiAL Calcdlus (q.v.) furnishes a simple and
elegant proof of the formulse for the areas of a circle and a sector.
If y=^z) be the equation to a plane curve referred to rectangular
Fig. 18.
Fig. 19.
Fig. 20.
axes, then the area bctwsen the cnrre, the, axis of x, and two
ordinates corresponding to the abscissa a and b is represented by
the iut^ral
/
<t>{x)dx.
For example, let AGP (fig. 20) be 6, then area of circle
= -2/ rf*--5—=Tr' as before.
The area of 3 sector can be found in a similar manner.
B, The Parabola.
§ 48. Length of an Arc of any Plane Curve. — If a plane cnrve b»
referred to rectangular axes, then the length of any arc of tha
curve
-/i -(!)■!'-/{. H-(S)i'4
taken between proper limits, i,c., the extremities of the arc Se6
IKFINITESIUAI. C\ICVLVS.
' 47. Arc of a Parabola. — Let the axes of coonlinates be the axis
Let X and y be the coordinates of P (fig. 20), then if OP=r the
equation to the circle isy''=r'-r', and therefore
Q'
Fig. 21.
of X and the tangent at the vertex A (fig. 21), then, the equation
to the paialxila being i/'=2ma:, where «i=2a=| latna rectum, w»
have
-;- =—, andhence
d'j m
.=ar^A^"|l.|,ji^
„yi'^y;+"t') m j^^ /'yl-^^/y;+"^' i .
therefore whole arc PAP'=-2!-v'p:f^ + TOiog,f?l±^M±^Y
Since y2>=2»nxi, the formula may be written
arc PAF=VSJTP; + lI log, /2^i + V'<^i + vA .
§ 48. Area of a Parabola.— Taking the equation to the parabola
in the form ir=ipx, we get
area of segment PAP' (fig. 21) =2/ i^Jpxdx
1^1=^
area of quadrant AOB =f
^ oL^"" r + 2
and therefore area of whole circle =nr'.
§ 45. If the equation to a plane carve be given in polar coordi-
natca, the area bounded by two radii and the curve is equal to
From these formtilx we see that the area of a parabolic segmesit
varies directly as the cube of the square
root of the abscissa, and directly as the
cube of the ordinate, and that it is equal
to i rectangle PQQ'P, or | triangle PTF
A similar relatioa holds for the segment
cut off by any chord, and thus the area of
any parabolic segment can be determined in
terms of any data that are sufficient to de-
termine the segment
§ 49. Areir. of a Parabolic Zone. — Let
PM (fig. 22) =y„ QN-y„, AM=x„ AN-a;^,
and let the ordinates be inclined to the axis
a*^ an angle a.
I Area of zone PQCT - segment PAP
- segment QAQ'
Zp
3^v<fi>.
where 9| and 6^ an tlie Talues of 6 cancsponding to the limiting
.ndii.
Now j/J = 4pi, and yl = ipx^, thereiore
y;-y;
substitnting for; we have area of zone
= S(x.-xj('4^nsin«=j5!^
Mxi-x^
C. The Ellipse.
§ 60. Circumference of an Ellipse. — The equation to the elUpeai
being -= -t- -1^ » 1 , whercaand i&re thesemiazes, we have
- a' tr
20
MENSURx\TION
are 01 ouadrant AB =
:, >nd therefore (fig. 23)
i.
dx " a'y
_ /"a 1 g' - cV
7o ( a-' -a:-'"
This inteeral may lio shown to be equal to the series
1.3=. 5c«
dx, where c'
Yl -il-Lii^
r^, 2" 2^ . 4- "
2- . 4'
&c.
jB rapidly converging series when « is a small fraction.
By taking more and nioro
terms of the above series we can
appro.ximate as nearly as we
please to the circumference of an
ellipse. For example, we have
quadrant AB
to a first approximation;
lieiicewholo circumference ^'
,=,{(M+(?^p nearly. Fig. 2a
§ 51. ^rea of an JSUipse. —We have at once
area = 4/ ydxi = — / \/d' - x-dx .
'0 "■Jo
fiut
t/" Vo=-
.Thus,
irdx is the area of the quadrant of a circle of radios
area of ellipse = 4 — (§ 44)
-- The following proof is worth the reader's attention. By a well-
'known theorem in conic sections the orthogonal projection of a
circle on a given plane is an ellipse. Now, if A denote the area of
any plane figure, A' the area of the projected figure, and 0 the angle
between the plane;? it can easily be shown, by dividing the two
areas by planes indefinitely near to each other and perpendicular
to the common section of the planes, that
Acos0 = A'.
In the case of the circle and ellipse A=jra^ and cos9= — ;
hence area of ellipse = iru' x — = iraJ .
§ 52. ArMi of an Ellipse in terms of a Fair of Conjugate Diame-
ters,— Let a' and 6' denote the seraicoujugate diameters, and a the
angle between them, then by an elementary property of the ellipse
ab = a'b's\na;
hence area of ellipse—ira'd'sina.
D. The Hyperhola,
% 53. Area of a Segiiieit of an ffyperbola.—Tbe equation of an
hyperbola being — r - ^= ^ > ^^ htLve
If the axes of coordinates be inclined at an angle a, we.moltipl^
the above results by sino to obtain the correct areas'
('ig. 24.
Fig. 25.
y=— Var'-o= ; hence (fig. 2'.
erea of the segment PAP = 2 — / "^x'-a'dx
-i,y,-aMog.^a.+a.^
, § H7Arca of a Sector of an Hijperhola. — The sector PAP'C is
iequal to triangle PCP'- segment PAP'
'Xai- j Xi!/i - aMog,^^ + ^!-^ I
=„Mog.(^ + ^)
, § 55. Area of a Zone of an Hyperhola. — In fig. 24 the zone
PFQ'Q
-segment QAQ'-segmo'-t PAP'
=a.,,y,-aMog,(|rf)-.,,. + aMog,(S + ^)
..,y,-..y,-aMog,(5gg), where
By y, and ij, 2/j are the coordinates of P ana Q respectively.
§ 56. Area hounded hy an Hyperhola and its Asymptotes, — The
equation of an hyperbola referred to its asymptotes is of the form
Let CM' (fig. 25)=«,, CM = ^„, Q'M'=i/i,Q M=j/;a_then, if a I»
the angle between the asymptotes,
area of Q1IM'Q'= / ^'fsmoax
= i?s,ma/ ' — = (rsmolog,( — ) = casino log,( — I »
7x2 x °\X2J Wi/
since x., = — anda-g^ — .
. a' + 6' J . 2ab , ,, .
Now <?•=' — 7 — and sino=-j— p , and thr.retoro
(a) a.Te^=iab\og,(^^)=iahlos.(^^\
Again, let MM'=a;i-Zj=i>, then
c-=x,y,=XM,=-^^^^ , therefore ■
(S) QMM'Q'= P&log,fS.^sina=H!^ log/ i^) in«-.
Again, since
4a^!/iSina = Jc'sina-JXoVjSina ,
we have triangle QCM = Q'CM', and hence
the sector QCQ' = QMM'Q'.
The corresponding results for a rectangular hyperbola are ob-
tained by substituting in the above formulae ia^ for c^ and 1 fot
sino.
Section IIL — Plake Ikregulah, KEcxiLrNEAL, and \jTra.yi-
LINEAL Figures.
A. Irregular Rcclilincal Figures,
§ 67. The area of any irregular polygon can be found by dividing
it into triangles, trapeziums, kc, in the most convenient manner,
and adding together all the areas. Fop example,
ABCDEF (fig. 26) = CKB + BKHA + AHF + FGE + EaiD + Dia'
Fig. 26. Fig. 27.
It may sometimes happen that some of the component figures
have to be subtracted instead of added ; for example,
ABODE (fig. 27) = AFHE + BCG-AFGB-EDH.
§ 58. Again, the irregular rectilineal. figure PjPj . . . PjPj (fig.
28) can be broken up into a .scries of triangles and-trapeziams a»
shown in the figure, and hence its area can be found.
§ 59. A figure made up of straight lines may be measured by
cutting it up into triangles by lines drawn from some one vortex to
the others. For cxamiile (fig. 29),
ABCDEF = ABC + ACD + ADE + AEF.
M E N S U RAT ION
21
it the polygon bs concave some of the triangles will hare to be
jnbtracted.
Fig. 28. Fig. 29.
§ 60. Area of a Polygon in terms of the Coordinates of its Angular
Points. — Let the coordi-
nates of P, Q, R (fi«. 30) bo
(ii, Vi). (a^s. J/s). and {x.„ i/,)
roapcctively, and let tho
axes be inclined at an angle
B. Draw PL, Qll, and RN
parallel to OY, then
LM-OM-OL-Xj-x,,
MN-0N-0M=X3-a;j, _
«nd QT" L M
NL-ON-OL-Xa-Xi. Fig. 30.
Now PQR-PLMQ + QMNE-PLNR.
Bot PLMQ = PLM + QMP = PLM + QLM
-.iPL-LMsino + 4QM-LMsina80°-o)(§9, (3^
-i(=:i-=;i)(yi + !/2)sino.
Similarly QM'S'B,-iiXi-x,){7j,+y,)sma,
•od PLNR - 1(^3 - Xi)(i/a + yi) sin a ; hence
areaof PQR-isina{)/i(z3-Xj) + y,(x3-x,) + y,(x,-Xj)};
or in the notation of determinants
•-isina 111
Vi Vi Vz I
Wlien the axes are rectangnlar sina=8in90°"l, and ihe formnla
for the area becomes
i{y,(Z3-a;3) + 2/j(x3-x,) + 2/3(x,-a:s)}
'i 1 1 1
Xi Xj X3
Vi Vi Vi
§ 61. The area of any rectilineal figure of n eides can be found by
taking any point within the figure and joining it to the n vertices
€f the figure, thus dividing it into n triangles the area of each of
vhich can be obtained as in the preceding case.
Wo may, however, find the area of the. figure directly.
For example, in fig. 31
PQ RST - PPTT + TTS'S + SS'R'K - EE'Q'Q - QQTP,
and in fig. 32
PQRSTU = PP'U'U-I- RE'Q'Q + TT'S'S - PP'Q'Q - RR'S'S - TTTJ'U.
V
T
.
3
P
L
>
^
R
C)
[>'i
r Q-£
V X
Fig. 31.
PR'Q' Tar
fig. 32.
B. Irregular Ourvilineal Figures.
§ 62. iength of any Curve. — If we divide the given arc into an
even number of intervals and re- jj
gard these as approximately circu-
lar, we can find an approximal^on
to the length of the arc by means
of Huygens's formula, § 32. For
•xample, if we divide ABC (fig. 83)
into four parts in D, B, and E, and
draw the chords AD, AB, DB, BE,
BC, and EC, then
arc AC - AD + DB + BE -t- EC -h |( AD -f DB -f BE -H EC - AB - BC)
approximately.
Pig. 33.
r or other methoos of approximation, see Rankine's Hules ani
Tables.
§ 63. Area of an Irregular Curvilineal Fig^ire. — For rough ap-
proximations the following, called the traoezoidal method, may be
used: —
Divide AjAn (fig. 3i) into n equal parts, and through the pointa
Fig. 34.
of division draw the ordinates, called by surveyors offsets, AiP,,
A,Pj, &c.
Let AjP, "=s, , AjPj-»,, &c., AnPn-<>u and
A^A.^^k^A^■= , , . -=An-iAn = a.
Join P1P5, PjP3, kc, then the area of the polygon A,A„P„P,P,
"AiAjPjl'i-l-AjAaPsPj-l- . . .-. -l-A„.iA„P„P„.i
= io(»l + »s) + 4«CSa + «3)+ • • • • +ia(Sn-l + »n)(§ 1». a)
'=o{i(«i + »«) + «3 + *a+ • • • •+»»-!}•
If we take n sufficiently great the difference between the area ol
the polygon and the curvilineal figure can be made as small as we
please, in other words, the smaller we make a the more accurately
will the above formula represent the area of the cuivUineal figure.
Tho curve may either be ^
wholly convex or wholly concave p, C p D.
to the line A,A„, or partly con- r?^^5p
vex and partly concave. " '^ — ^ ' '
§ 64. Simpson's ijufc— Let
AjAn (fig. 34) be divided into
an cv«?i- number of equal parts,
and as before through the points
of division draw the ordinates
A P A P &c
'li'tA'.A'JPaPi^figs. 35, 36)bo k . a. A, A. _..
a part of the figure thus di-
vided; join PjPj, and through j-;™ 35, pjg. 38.
Pj draw BC parallel to P,P3 to "
meet AiP, in B and A3P3 in C. Conceive a parabola to be drawn
through PjPjPs haviug its axis parallel to the ordinates, theu
A,PiPjP3A3 = trapezi.*.m AiPiDPjAaiparabolic segment PiPjP,
= c(«,-f S3)±ia{«a~i(Si + »3)}=J«(''i + ^*a + »3)-
Now when the points P„P;,P3 are near each other tho parabolic
curve will coincide very nearly with the given curve ; hence
AiPjPjPaAa" Jo(s, -t- 4S3 + S3) very nearly.
Similarly AsP^e^/i.ti-'iaiSi+iSt+s^), &c. ;
hence whole area of figure
= ia{si + Sn + 2{S3 + s^+ .... +s„.,) + i{h + ^i+ • • ■ • +»»-')};
whence the rule:— add together the two extreme ordinates, twico
the sum of the intermediate odd ordinates, and four times the sum
of the even ones, and multiply this result by one-third of the common
distance between the ordiuates; the result is the area, — accurately if
the curved boundary be the arc of a parabola, iu other cases ap-
proximately. ,
The curve may either be wholly convex or wholly concave to tuB
line A,A„, or partly convex and partly concav«, provided in the
latter case the points of contrary fiexure occur only at the odd
ordinates, for otherwise the intermediate arcs could not be even
approximately parabolic. When points of contrary flexure occur
ordinates may bo drawn at these points, and the intermediate arcs
being found separately may be added to obtain the whole area.
§ 65. In the two preceding sections we investigated two formnla
for approximating to the areas of cnrvilinear figures. ^ Wfe no^
proceed to consider the subject more generally.
Ai Ap Ap
Ai»»i^
Fig. 37.
Let the equation to the curve PiP,P„+i (fig. 87) ngree with thS]
122
ENSURATION
ieqDation!/=A + Bz+Cs'+ .... +K3"forn+l points between
P, and Pn+i, then the area of the cnrvilinear figure bounded by the
Wraight lines A,P,, AiA„+i, and A„+iP„+i and the curve PiP„+i
mill agree very nearly with the curvilinear figure bounded by the
tiioe straight lines and the curve whose equation i3y = A + Bz +
Ci~ +....+ Kx", and the greater the number of common points
the closer will be the agreement.
I Let A,A„+i be divided into n equal partj, each equal to h, then
'AiA„+i=7iA. _ Now
\vhena=0, y-=y, = A;
yihenx'-k, y~y^=A + 'Bh+Ch-+ .... +KA";
.whenz-2A, j/-y3=A + B(2ft) + C(2A)»+
yihenx^ph, y= yr+\ = k-\-'B{ph) + C{pK)- +
when a=KA, !/=»;„+i = A + B(n7t) + C(n7j)= +
, . +K(n;i.)».
From these )i + l equations the m + 1 quantities A, B E
can be determined as functions of 7„ !/j, .... i/n+i , .lud ft.
I Next let A,Ar,+i bs divided into m equal parts each equal to h.
Thus mh=nh and hence h, = — .
Now
iBut
the area of the rectangle ApAp+iP,R=A,Ap+ix A,P,.
■A,Fy = r/p - A + B(pA) + CtpA)' +
p.nh
i^^r
. . +K{ph)"
and
therefore area of A,R
■Tih\ — + Bnh-^,+Cn%'—,+ .
I m m^ m'
fleace the area of the whole figure
+ Kn»A'
m"+' 1
0 ^p=l I m in? ■ m* m"+' J
nh\ A
So
RtiA
-T,+
Cn'K-
S.,
where S„=l»+2'>+3"+ . . +m».
Now if we take the limit of each of the terms
§1 fi. i ^"
m * m" * m-* * ■ • • • ^„+i »
we obliin area of curviliiicajr figure
, ( . B , C „,, K
= »« < A+-;^ft+-^7l-/l^+ . .
l+l
fi^h"
From this general result we can deduce " Simpson's Kule " and
also another rule called "Weddle's Rule."
I TJhus let n — 2; that is, assume that the curve under consideration
i^as three points in common with the curve whose equation is
ly—A+Ba+Cx", i.e., with a parabola, then
2/3=A + BA +Ch?,
2/3=A + 2BA + 4CA».
^ow the area is approximately
= 2A{A+4B2A+1C2=A=}
= J7»{6A+CB/» + 8CA=}
■=^{^1 + 41/34-2/3}, Simpson's Eiilj.
If we now put 71=6, we have area of curvilinear figure
- 6A { A + iB6A+ SC6%s + }C6%' + JEC'A* + JF6=A= + ^6%"} .
^ow »/i=A,
j/3=A+B/i+C;i-+ . .-. . +Gh\
t/7=A + B(6A) + C(6A)'+ .... C(6i)».
From this system of equations we can determine A, B, C, . . . G,
{and substituting the values so obtained in the above expression we
obtiun the following remarkable formula for the approximate area:
area=AA{(yi+s'3+y»+y7)+y4+5Cy3+y4+y6)} .
This formnla, called Weddle's Enle, gives the closest approximatioo
to the curvilinear area that can be obtained x
by any simple rule.
Wo are now in a position to find the
approximate area of any irregular plane
figure. For the given figure can bo
divided into plane rectilinear and cur-
vilinear figures, the areas of which can
be separately determined by the rules
already given. For example, APQBS
= ABC -f APD + BEG - DQB - ASC .
Fig. 38.
PAET II. SOLIDS.
Section I. Solids contained by Planes.
A. Priims, Pyramids, and Pristnatoids.
§ 6C. Volume of a Rigid Prism. —First let the prism be a rect-
angular parallelepiped (fig. 39), and _
let the side AB contain a units of
length, BC b units of length, and
CD 0 units of length. If we divide
AB into a equal parts, BC into 6
equal parts, and CD into c .equal
parts, and if, through the points of
division we draw planes parallel to
the sides of the parallelepiped, these
planes will divide it into a series
of parallelepipeds, whose edges are
each equal to the unit of length.
Each horizontal layer contains ab
of these cubes, and since there are c
layers the whole number of cubes
will be ahc. But each of these is the unit of volume, and therefo*
volume of AECD = a6c = a5 X c = area of base ABC x altitude c ^
In the above demonstration we have assumed the edges to be
commensurable, but from § 2 it follows that the proof will hold
also when the edges are ' incommensurable. It the parallelepiped
be cut by a plane BGE it will be divided into two equal triangular
right prisms, and hence
volumeof righttriangularpnsm- 4(zi x <;=areaof its base x altitude. 1
Since every prism can be divided into triangular prisms as in fig.:
40, we have at once
volume of right prism A'ABCDE=A'ABC-4- A'ACD-^A'ADE
= ABC X BB' -I- ACD X CC -H ADE X DD'
= (ABC-^ ACD-1- ADE) x altitude
(since BB'=CC'=DD' = altitude)
-area of base ABODE x altitude.
Fig. 39.
Fig. 40.
§ 67. Volume of an Oblique /Vtjm.— Draw the right section
a"B"C"D"E" (fig. 41), and let A' denote its area and A the area of
the base A'B'C'JJ'E'. Let t denote the length of the prism, h its
altitude, and a the angle between the planes A'B'C'D'E' and
A"B"0"D"E". _ i
Conceive the part above the right section placed at the other
extremity of the prism. Then we have a right ;'rism, whoss
volume-A'x/ (§ 66); butA'=Aco3 o, since A*^ is the projection)
of A (§ 61),
and I— ; hence
h .
cosa '
vol«me'=A'xi«"Acosax — AxA ;
or the volume of any prism is equal to the area of its base militi*
plied by its altitude.
MENSURATION
23
g 48. Surfact of a Prism, — Since the lines A"B", E"C'', tc. (fij».
f41)i which make up the perimeter of the right section are all n\
one plane perpendicular to the parallel edges A' A'", B'B'", He, they
• re perpendicular to these edges and are therefore the altitudes of
the parallelograms A'B'B'"A, B'CC"'B"', Uc, respectively. The
lateral surface of the prism is equal to the sum of these parallclo-
gnuus, and therefore
-A'A"'xA"B" + B'B'xB"C"+
-A'A"'(A"B' + B"C"+ ), -
«inco A'A'"=B'B"'-ic.;
or the lateral surface of any prism is equal to the perimeter oi j'a
right section multiplied by the length of the prism.
If the prism be i-ight, that is, if the faces be perpcndicnler to tt'
base, then its lateral surface is equal to the perimeter of its bai i
multiplied by its length.
The whole surface of any prism is obtained by adding to th;
lateral surface the areas of its bases.
§ G9. If the prism be regular, that is, if tho bases bo regular
polygons, then
area of base-o'x Acot-5!i- (§ 18, y) where n is the nnmber
of sides each of length a, and therefore .
volume =
,.180°
xft,
where h is the altitude of the prism.
Again, if tlie prism be right and regular, then
its lateral surface = nah + 2a' x — cot .
§ 70. Voluine of a Pyramid. —Let TABC (fig. 42) be for sim-
Elicity a triangular pyramid. Divide VA into n equal portions, and
brough the points of section draw
filancs parallel to the base ABC, and
hrough BC and through the inter-
•ections of these planes with VBC draw
S lanes parallel to VA. Let k denote
le altitude of the pyramid, then the
distance of the base of the r"* prism
trom the vertex Y
A
-rx — ,
and, if A denote the area of ABC, we jC
have
base of r"* prism r'A' 1 r"
A» n"
Fig. 42.
■nee, by a well-known theorem in solid
geometry, the areas of sections of a pyramid made by planes parallel
u the base are proportional to the squares of their altitudes.
Thus we have
base of r"* prism «<—^ A, and therefore
(§ 67)
TherefoiB volnme of whole pyramid
-aaL„
n(n + l)(27t + l) ^^,
0 6n^ ~
i;
er the volume of any pyramid is equal to one-third of the area of its
base multiplied by its height.
From this we see that pyramids on equal bases are to one another
as their altitudes.
If the pyramid bo regular, that is, if its base be a regular polygon
the perpendicular through whose centre passes through the vertex,
its volume = J x o' x -2.cot xh
4 n
%1\.- Surface of a R'.giilar Pyramid. — The lateral surface of the
regular pyramid VABCDEF (fig. 43) is equal to the sum of the areas
of the n congruent triangles which make up the lateral surface of
the pyramid.
Now area of triangle VAJS^JAB x TO; hence whole lateral sur-
face—JnABVG— InoJ, where I is the slant height and a the length
ef the side of the base.
Again, if VO — A = altitude of pyramid, we have
theiefore whole surface^oaso+latersl surface
=«» X -fcotl^V 4«« yA'-^^cot»^
Fig. 43.
§ 72. The Prismaloid. — If we have a polyhedron whose oases are'
two polygons in parallel planes, the number of sides in each being!
the same or diflerent, and if we so join the vertices of these bases'
that each line in
order forms atrianglo
with the preceding
lino and one side of
either base, the figure
GO formed is c^ed
a "prismatoid," and
holds in stereometry
a position similar to
that of the trapezium
in planimetry. To
make the investiga-
tion of the volume
of the prismatoid as
simple as possible,
wo take the case
where the lower base
is a polygon of four
and the upper one oi
three sides.
Let ABCDEFG
(fig. 44) be the pris-
matoid, of which
ABC or A, is the
upper and DEFG or
A5 the lower base,
and let HLM be the Fig- ^*-
section equidistant from the bases. Take any point P in this
section and join it to the corners of the prismatoid. We thus
divide the polyhedron into two pyramids PABC and PDEFO,!
and a series of polyhedra of which CPDE may be taken as a
specimen.
Let A be the altitude of the prismatoid, then {h isthealtitnosof
each of the pyramids PABC, PDEFG, and hence
volume pf PABC =JAA,, and
volume of PDEFG =JA A3
Again join PH, PL, and LD, then
volume of CPDE = 2 volume of CPDL,
since DE=2HL,
and volume of CPDL =2 volume of CPHL,
hence volume of CPDE=4 volume of CPHL.
Now volume of CPHL = JA x area of HLP, and therefore volnmo
of CPDE-JA X area of HLP.
Similarly the volume of every such polyhedron is JA x the area
of its on-n porlion of the middle section. Hence if A^ denote tha
area of the middle section we hare
volume of prismatoid = JAA, + J AAj + JAA,
-iA(A, + 4A,-KA3),
§ 73. Volume of the Frustum of a Pyramid.— l^t A'A'"B'B"'(3'C"'j
(fig. 45) be a frustum of the pyramid VATB'C, and let A, and A,'
denote the areas of the ends A'B'C, A"'B"'C" respectively. Let
VP - a; = altitude of pyramid VA"T3"'C"', and let PQ - A - altitude ofl
ftnstnm.
N"' (sTa)'-^' whence x-^*'^^^.
2i
t«[:e_^n:s_u R a t i o n
(Again frustum- VA'B'C - VA"'B"'C"
ftVA,
VA, - VA;
0}
<VAi-VA
_^ /-JMA. + VAiAj + Aj);
pTonnnls which applies to the frusta of all pyramids regular and
irregnlar. _ ^
The ahove result may be otherwise expressed. For, let A'B — O]
and A"'B"'-a3, then, if A"B"C" be a section equidistant from the
tends of the frustum, A"B" = Oj = ^(aj + aj).
Now Aj=jmJ and A^=pal (see § 70) ;
Jience As=areaof A"B"C"=pa5=^[ 2li^ J , which gives
4A5 =pa] + 2pa^a^ +pal = Aj + 2VA1A3 + A3 ;
^erefore volume of frustum
^ -iA(2Ai + 2VA7Aa + 2A3) = j;j(Ai + 4As, + A3); ^
jbr the volume of the frustum of a pyramid is obtained by adding
fthe areas of the ends to four
kimes the area of the middle
Isection, and multiplying the
»um by one-sixth of the alti-.
Itade.
The above result can be oh-'
[tained at once from § 72, since
|A'B'CA"'B"'C"' is a prismatoid
iwith similar bases.
§ 74. Surface 0/ the Frustum
^f a Regular Pyramid. — In fig.
&6 let the perimeter of A, =Pi,
^hat of A^—Pi, and that of
Xb-t-'Pi, ^^^ 1^' ^^' = ^1
fVD"'■=^J, and therefore DD"'=
!VD' - VD"' = i, - ^3 = Z. The ^ ^r,\
lateral surface of the frustum la o \
tqual to the diflFerence between the lateral surfaces of the pyramids
IVA'B'C' and VA"'B"'C"',
bSt, sinc7iL = f!l_^- = Pl, wehaveZ,=-2i^and Jj— ^s^ .
l^ 03 Mtj p^' Pi-i>, ",?!-?«
[therefore lateral surface of frustum
Er the lateral surface of the frustum of a regular pyramid is equal
to the product of the slant height and the perimeter of the section
jequidistant from the ends.
Otherwise. — The top and base being regular polygons, the inclined
?aces are congruent trapeziums. Let I be the height of each
{trapezium, and let there be n of them, then
§ 77. If the prism be right or'ablique, the vftluine'of a frustum ii|
equal to one-third of the area of its right section multiplied by thai
sum of the parallel edges. For divide tho frustum aA'B'C (Sg.l
47) into two frusta by a plane A"B"C" of area A at right angles^
to the edges, then
AA'B'C - AA"B"C " + A"A'B'C
- } A( AA" -t- BB" -f CC") -h JA (A' A" -H B'B" + CC") ,
= J A(AA" -H BB" -H CC" -I- A''A" -H B'B" + GG')f
'■=iA(AA' + BB'-HCC).
Again, since every prism can be divided into triangular prisms, ,
we can find by repeated applications of the above proposition the
volume of the frustum of any prism whatever. _ For example, if
area of eacn face =
2\n «/•
fend therefore the area of lateral surface = -5- (ft + Pa) = ?Pj ■
.B'
•:. — -iCF
t'
• § 76. If h, the altitude of the frustum be given, we deduce the
giant height and then proceed as before. Thus bt VP—Aj,
^Q=Ai, and using the same notation as in §| 72, 73, and 74 we
Ihave -
^-*l_ S—, whichgive3A,=<5l&-^L-2!^ .-,
ligkiil* ^;=A;-^ia;cot^ — .ai>d;=('5l^l2a')z,;
■n \ "1 /
(whence I is known since ij is known in terms of h.
When the pyramid is irregu-
lar the lateral planes are non-
fcongruent trapeziums, the areas of
which can be found separately by
1 12, and hence the whole surface.
§ 76. Folume of the Frustum of
b Triangular Prism. — Let A denote
|the area of ABC (fig. 46), and let
lAi, ^, A3 be the altitudes of A',
IB , C respectively with reference to
[the plane ABC. Divide the frustum
into three pyramids B'A'AC, B'ABO,
land B'A'CO' by the planes B'AC
knd B'A'O. These three pyramids
are respectively equal to BA'AC,
B'ABC, and ABCC;
hence volume cl frustum -iAiA + Sft,A + Jft^A
-^A(A.4.A..^^. .
Fig. 46.
Fig. 47. Fig. 48.
the base of the frustum 'of "alright prism AA'B'CD' (fig. 48?
be a rectangle 12 feet by 6 feet, and the parallel edges in ordtfl
6, 4, 10, and 12 feet, then
A — area of base = 12 x 6 >= 72 square feet
Frnstnm - ABC A'B'C + ADCAD'C
- S X i A(AA' + BB' + CC) -(■ 5 X J A(A A' + CC + DD") .
- i A (2 AA' -1- 2CC' -^ BB' -I- DD') = 676.
§ 78. Volume of a
JVedge.—The wedge (fig.
49) being merely the
frustum of a triangular
prism, we have at once
volume — iA(FE
-hAD-l-BC),
wnere A is the area of its
right section ; otherwise,
the .wedge may be con-
sidered a prismatoid pj ^j_
whose upper base b a .
straight line, and hence its volume = iA(4A3-)-A3), since Ai=0.
B. Regular Polyhedra. ^
§ 79. The regular polyhedra are five in number," namely, th^
ielrahedron, cube, octahedron, dodecahedron, and icosahtdron, whose
solid angles are formed respectively by three equilateral triangles,
three squares, four equilateral triangles, three pentagons, and fivs
equilateral triangles.
Since a regular polyhedron admits of having a sphere inscribed]
within it and described about it, it can easily be shown that the,
volume of the polyhedron
and from § 18, 7, it follows that the surface of the polyhedron^
where 7~the number effaces, '
m — tho number of faces in each solid angle;
7i-=the number of ctlges in each face,
and a = the length of each side.
The following table contains the surfaces and volumes for tli^
five regular polyhedra whose edge is 1.
Polyhedron.
Snrjacc.
Volumo.
I -TS-.TOOS
<1-0000000
n'464I0I(!
!1«4f.7788
80002540
01178511
l-OOOOOOO
0-4714(143
7-6631185
31816950
MENSURATION
25
frhe^ surface and volume of a regular polyhedron whose edge is
U is obtained by multiplying the surface and volume of a similar
feolyhedron whose edge is 1 by 0= and a' respectively.
1 Section II. Solids contained hy Surfaces ivsion aee not
ALL Planes.
A. The Cylinder.
S 80. Volume 0/ a C<jlindcr (fig. 50).— Inscribe in the cylinder a
polyonal prism of which the number of sides may be increased
uidefinitely. Then in the limit the base pf the prism becomes the
b.iso of the cylinder, and the volume of the prism the volume of
the cylinder. Now by § C7 we have
volume of prism = area of base x altitude ;
hence volume of cylinder = area of base x altitude.
§ 81. Surfaec of a Eight Cylinder. — As above, in the limit the
bnse of the prism becomes the base of the cylinder, and the surface
of the prism the surface of the cylinder. Now the lateral suiiace
of prism
= perimeter of right section x length
~ perimeter of base x length, in the case cf a right prism (§ 68);
hence lateral surface of right cylinder -circumference of base
X length.
V
Fig. 50. Fig. 51.
B. The Coiie.
% 82. Volume of a Cone (fig. 51). — Inscribe within the cone a
pyramid of which the number of sides may be indefinitely in-
cri'ased, then in the limit the base of the pyramid becomes the base
of the oone and the volume of the pyrj.raid the volume of the cone.
By § 70 volume of pjTamiJ — i base x altitude,
and hence volume of cone — 3 base x altitude.
§ 83. Vohmc of the Frxislum of a Cone.— From § 73, we find that
the volume of the frustum of a pyramid
= JA(Ai + VA;A; + A3y;
hence, since in the limit the frustum of the pyramid becomes the
frustum of the coue, we have
volume of conical frustum = 5^ ( A, + VAjAj + A3) ,
wliere A, and A3 are the areas of the terminating planes of the
frustum.
Lot the terminating planes be circles of raOii r^ and r^, then
volume of fmstum
= JA (irrj + irrir, + «■•) = JirA (rj + rir3+ rf) .
Again, by the same section we have
volume of frustum of pyramid=JA(A, + 4A2 + A3),
therefore volume of conical frustum = -Jrfi (rj + 4r^ + rj) ,
where r. is the radius of the circular section parallel to the ter-
minating planes and equidistant from them.
§ 84. Surfaee of a Right Cone. — Thrf lateral surface of a regular
pyiamid is by § 71
= J perimeter of base x slant height ;
hence, since in the limit the surface of the pyramid becomes the sur-
face of the cone, tlie lateral surface of a right cone is equal to half
the circumference of its base multiplied by the slant height.
Thus the lateral surface of a right cone of slant height I and the
radius of whose base is r is equal to
4x27rrxZ = 7rrZ,
and whole surface = lateral surface -f area of base
~ iTT^ + irr-
=.nr{l-\-r).
Again, if A, the altitude of the cone, ne given, wo have
and therefore whole surfacc=-7rr(VA' + r--Hr).
§85. Surf ace of '.Iv, Frustum of n. Eight Cone. — The hteral surface
of the frustum of a regular pyramid is eaual to the product of the
alant height and the perimeter of its middle section (§ 74) ; hence
in the limit wo find that tlie lateral surface of (he frustum of a
right cone is equal to the prodtict of its slant hci;;lit and the cir-
cumference of the section equidistant from its parallel f.iccs.
Lot T-j and r, denote the nidii of the ends of tUo frustum, and I
the length of the slant height, then
'■3 ■= i(''i + ^i) = radius of middle section,
and therefore
lateral surface — 2irr3 x ! = 27r x J(r,-H'3) x Z — irJ(r,-t-rj) ,
and whole surface = Trr ; + T?(r, + r^ + irr] .
If A, the altitude of the frustum, be given, we have
Z=.V/i=-Kr,-r,)i.
C. Tlie Sphere.
§ 86. Surfaee of a Spherical
Zone.— Let AB ("fig. 52) bo a
small arc of tlie sphere, and
let AA', BB' be perpendicular
to the axis XX', to find the
surface of the zone generated
by the arc AB. Join AB, and
draw OP perpendicular to AB, _^|
BD par.alh-1 to XX', and PP' •'^|
parallel to AA' or BB'. The
chord AB generates the frustum
of a cone, whose lateral surface
-2tPP'xAB.
But, since the triangles ABD
and OPP' are similar,
AB^OP
BD PP' '
therefore area of conical frustum - 2n-. OP. BD = 2ir. OP. A'B'.
Similarly the area of the frustum generated by BC = 2:r.0Q.B'C'.
But in the limit when the chords AB, BC, &c. , are indefinitely
diminished, the perpendiculars OP, OQ, &c., become each = r, and
hence by summing all the areas we get in the limit
area of zone — 2irr x (projection of arc on axis of revolution).
Hence the convex surface of a sefxmont of a sphere is equal to the
circumference of a great circle multiplied by the height of tho seg-
ment or zone.
g 87. Surface of a Splim. — Tho whole sphere being a zone
whose height is 2r, wo obtain at once
surface of sphere — 2irr x 2r=» 4Trr^ ;
or the surface of a sphere is equal to four great circles.
The total surface of tho cylinder circumscribing tlie sphere of
radius r is Gn-r", hence the surface cf the sphere — § surface of cir-
cumscribing cylinder.
§ 83. Surfaec of a Lur^e, a Spherical Triangle^ and a Sphericdt
Polygon. — It is siiowii in spherical trigonometry that
(a) the area of a lune included between two great circles of A
sphere of radius r, and whoso inclinatiou is 0 radians, is
2fl;~;
{ff) the area of a spherical triangle whoso angles are A, B, C is
(A-l-B + C--ir)r=j
(7) the area of a spherical polygon of r sides is
{P-()--2)ir}r', where P is the sum of its angles.
§ 89. Measurement of Solid Angles. — X convenient unit for tho
measurement of plane angles is llie "I'adian." If wo assume that
each unit of surface of a sjihcre subtends the same solid angle at the
centre, we can deduce a very convenient unit for the measurement
of solid angles. This unit, which has received the name " stera-
dian," we define to be the solid angle subtended at the centre of a
sphere by a portion of the surface whoso area is r-.
§ 90. Number of Stcradians in an Angle. — Let A be the angle at
the centre of a sphere, and let S bo the portion of the surface of the
sphere which it intercepts, then
number of stcradians in A S_
For example, if A be a plane solid angle, S = a hemisphere
-2irr=; hence the number of s'eradiatis
in a plane solid angle — — -=-^^-:^ = 2r,
and therefore the number of steradians in .
the solid angle at a point - 47r. This solid ^
angle is sometimes called a steregon.
Hence, if wo can find the .surface sub-
tended by any solid angle, we can always
find its magnitude in terms of the unit
solid angle.
§ 91. Volume of a Sphere.— Ut ABC ^
(fig. 53) be the quadrant of a circle, draw DB and T)C tangents to
it then, if AD be joiiied and the whole figure bo conceived U
XVL — 4
26
MENSURATION
(rotatint; round AB, ACD, ABC. an-l ABDC will generate i;conc,
I ft llcmi^pIle^e, and a cyliudcr ivspcctivcly.
Now diMW two paiallc". planes EFGH and E'F'G H' very near each
lothir and perpendicular to AB, an'' draw FF and GG' parallel to
AR, tlien, by § SO,
volume generated by EHH'E =iri!.H' x EE',
„ „ EGG'E' =irEG= x EE',
,1 „ EFF'E' -jrEF= x2E'.
Thus volume generated by EFF'E' + volume generated by EGG'E'
= t{EF= + EG-) X EE' = -^rCEA^ + EG=) x EE'
= ,r(AG=)xEE' = 7rEH"-xEE'
= volumc generated by EHH'E'.
Therefore in the limit, when the number of slices is indefinitely in-
creased, and their thickness indeQnitely diminished, we have volume
of cone generated by AF + volume of spherical zone generated by CG
- volume of cylinder generated by CH.
Let r = radius of sphere, /; = AE = height of zone ACGE, then
volume of cone = ^irh- x A = ^nh^, and
volume of cylinder = 7rr- x h,
therefore volume of spherical zone = wrh - Jj-A'
= 4^71(3^=-^.
The height of a hemisphere is r,
therefore volume of hemisphere = ^ttt (3r' - r^) =. |7rr' ,
»nd volume of whole sphere — ^Trr' ,
a result readily obtainable by the infinitesimal Calculus, or by
inscribing w-ithiu the spliere a series of triangular pyramids whose
.vertices all meet at the centre of the sphere, and the angles of whost
'bases all rest on the surface. In the limit the altitude of each
pyramid becomes the radius of the sphere, and the sum of the bases
of the pyramids the surface of the sphere ; hence
volume = IS X r - J X 47rr= x r= fxr' .
The volume of the circumscribing cylinder = «-=x2r = 2irr',
therefore volume of sphere - 1 volume of circumscribing cylinder.
§ 92. Let S denote the surface of a sphere and V its volume, then
from §5 87 and 91 we have
(a)7-
Vs
-'yf.x^^^
2V'
(j3lS = Vr(0V)=;
formula which give the radius in terms of the surface or volume, the
surface in terms of the volume, and the volume in terms of the
surface.
§ 93. Voluinc of a Spherical Shell. — Let r and r, denote the radii
of the two spheres, then
volume of shell •= V = JirrJ - Jirr'
= in-(r,-r)(r;-(-rir+r=)
Now letr, -r=A', then
V-J«-;7i('l+il + 4)
If h be small compared with rj, tnen r/rj is very nearly equal to 1,
and we have approximately
V = Jirr;/t(l + H-l) = 47rr;7i.
Again, if A he nearly equal to r,, r is very small, and rjri is also very
small, so that we have approximately
S4) be a
§ 94. Voluvic of a Spherical Segment. — Let CEC
Bection of a spherical segment whose
altitude RQ is p, then, if 0Q = /(,
volume of segment CRC' = volume of
hemisphere - volume of zone AA'C'C
^lnr'-Uh{S'-'-h^,%9\. g
-Jjr?)=(3r-;)).
If wo put;;"2>', we obtain as before
volume of sphere ■= ^ttt' .
Again if CQ = n , wo have
CQ- = o;-RQ.E'Q-j)(2r-i)),
R U
whence r=.^— ?^ ,
2p
Fig. 54
therefore relume of segment— iirp (SnJ +;)').
8 96. Volume of a Spherical Frustum.— \Yiu:n one of the termi-
nating planes pisses throudi the centre we have already foun4
that the volume
= Jji-;((r=-A=),
where h is its altitude. .,
Now suppose that neither of the terminating pianos passes through
the centre ; for exnmi)le, to find -'' ■> volume of the frustum BB'CCl
Let UQ = p and Kl* = y, then
Bb'C'C = segmcut RBB'- segment RCff
= irql,3al+q--j-hV>(.3l\+!r),
where o, and a» arc tlie radii of the ends C"C' and BB'.
Let q-p=h= height jf frustum, and, since, from the geometry <A
the figure,
a'+p- n:-t-i?-
2> 9
we have volume= J7r/i.{3(a; + a|) + A-},
a result which may also be obLained by considering BB'CC as th*
difference of tho iwo zodes AA'C'C and AA'B'B
D. Sjihcroid.
§ 96. Surf act of a Prolate Spheroid.— the prolate spheroid is thtf
solid generated by the revolution of an ellipse about its major axiaj
If S be the surface generated by an arc of the curve, then
S=27r/j/ k/'^ + ('^\^Xi taken between proper limits.
= 2r.
In the case before us
= 2iri- + 2?r-
where c is the eccentricity (Infinitesimal CALcnms, art 179).
§ 97. Surface of an Oblate Spheroid.— The oblate spheroid is th*
solid generated by the revolution of an ellipse about its minor axi»
(fig- 55).
Here surface =2ira- + «
-log,-
(iNFlNlTEdlSIAL CaLOULDS,
art. 179).
§ 98. Vohime of a Spheroid. — We have volume of prolate spheroid
.similarly vilume of oblate SDheroid=iiro-6.
Thus,
volume of prolate spheroia JTrao' _6_ .
volume of oblate spheroid Jjrct-'fi a
sphere described on major axis -Jira' a* .
prolate spheroid ^-rrab'^ b^
sphere described on minor axis JTrb"^ V^ ^
oblate spheroid ^nd-b a?
§99. Volume of a Segment of a Sphcrow.
(a) Tlie prolate sphcroid.—Thh segment is generated by tlift
revolution of AMP (tig. 23, p. 20) about AM, andlience
its volume = it/ y'dx = ir^ / '(2«r - a:=)<fa = -^ x — =- (So - A),N
where A is the origin and AM =■ h.
{$) The oblate spheroid. — The segment in this case is penerateff
by the revolution of BMP (fig. 55) ab-^ut BC. and hence
a'h'„
(t)
/•A ^2 /•li
it3Volume = ir/ jz-ox-tttj- / {2ox-
f)dx^
b^
(36-/1),
where B is the origin and BM = A.
§ 100. Volume of the Frustum of a
Spheroid when one of the Terminating
Planes passes through tlie Centre.
(a) 7'he prolate spheroid. — The frustum
in this case is generated by the revolution
of BCMP about CM (fig. ^3).
Now volume generated by BCMP
— volume generated by BCA
- volimio generated by PMA
, ,„ w 6-'A2
- Ixab- - y X -^(3a - A)
= JLx*I^'(3a=-i-=), where
i=CM=heightoffrustum = ii-A. Fig. 65.
(P) The oblate sithcroid.—'Wo can show in a similar manner,
that the volume generated in this cise
-^x^"(34='-t=).
The above formula; may bo put into another form. Thus, in the
case of the prolate spheroid, since the point P lies on the cllipsd
fc-ar'+a-y^ — rt'-t'-, wo have
j?j(j . »■ 1 _ (j-i^ ^ where 6, - PM , which gives
MENSUKATION
27
il^ence, bf sabstitntioD, the rolame of prolate (rustom
= J»i(26': + 6;).
^jimilarl; we can show that the volume of the oblcte frustum
where a, =■ I'M .
Ilbtae formolffi plaj an important part in the gauging of casks. -
E.' Paraboloid.
5 101. Surface of a ParaboloyJ. — Let the cqnation to the para-
%obi be y'^iax, and let the coordinates of P (fig. 21, p. 19) be «„
!y„ then the surface of the paraboloid generated by the reroJutiou
vl AM about AP
§ 102. Folume of a Paraboloid.— 'Viih tBe same notation wo
have
Tolame=ir/ y'dx^iTm/ xdx — J» x iaxi x x^ =iiryj x a, ;
or the volume c f a paraboloid generated by the revolution of a part
'cf a parabola between the vertex and any point is equal to half the
Volume of the circumscribing cylinder.
I § 103. If the coordinates of Q be x^, y^ then the volume of the
frustum PP'Q'Q
- Jir { yiSj - J/I^i } = 2iro(a:5 - xj ) = ii(y; + y ; )A ,
ihere ft-MN ; hence the vohime of the frustum of a paraboloid
IS equal to half the sum of the areas of its ends multipued by its
height
F. Ellipsoid,
i 104. Volwme of an Ellipsoid. — The equation to the ellipsoid
'Ming
3? ifi ^
— +— +— — 1 '
^e equation to the elliptic section at the distance z from the
'origin is
Now if. we draw an indefinite number of parallel planes per-
pendicular to the axis of z, each slice will be an infinitely thin
cylindrical plate, and accordingly the whole volume oX ihe eUipi>oia
—Jkdz, where A is the area of the elliptio section.
butA-iroi^l-.£.V§61
'therefore volume - iroy M__J(fe—firaie.
The sphere being an ellipsoid whose axes are all eqoal, we obtain
u before
volume of sphere= Jira'=}»r'.
G. ffyperboloid.
,- 1 105. Pblwme of an Hyperboloid. — The hyperboloid is generated
by the revolution of the hyperbolic segment ANP about AN (fig.
U, p. 20). If the coordinates of P be x^, y^ then
' volume of hyperboloid =iy ydx—r^i ^'(x'-o'jdr
'(3o+A),
V I
where 76-= AN ^a-i -a.'
Again, since z^ y^ is on the curve, we have
62
o'y;-6»(o+A)'= -o'i', which gives-
volume of hvDerboloid=^y!^ >
Za + h
2a + h '
H. Solids to which the " Prismmdal Formula " applies.
_ § 106. It was shown in § 72 that thn volumo nf any polyhedron
bounded by two parallel planes and by plane rectilinear figures
-i7i(Ai + 4A,-l-A3),
where A„ A3, ar.d Aj denote respectively the areas of the two ends
and of the middle section.
I We now proceed to show that the same formula determines the
volames of all solids bounded by two pirallel planes, provided tho
area of any section parallel to these planes can be expressed as a
r\ional integral algebraic function of the third degree in x, where
t is <;he distance, of <he section from either flauu.
Let <p(.x)=A + Bx+C3? + Thi?+ .... +Ka" denote the area
of the section in question. J
Now the solid between the sections ^(0) and <l>{i) is equal to the
solid between the sections <f.(0) and 4>(2) plus the solid between th«,
sections 0(2) and (p{i). Hence if the prismoidal formula is to hold!
in this case, we have
JA{«(O)+4#(2) + 0(4)}
=-hH<P{0)+i4>{l) + 'p{2)}+-^h{<t,{2) + if{3) + it>Wii
where h is the distance between the sections ^(0) and <pli)f''
Hence we have
0(0) - 40(1) + 60(2) - 40(3) + 0(4) =0.
Now 0(0)= A
— 40(1)=-4A-4B-4C-4D-4E- . . . .--4K
^60(2) = 6A + 12B + 2iC + 48D + 96E-r .... +6-2"K^
-40(3)-.-4A-12B-36C-lO8D-324E- .... -4-3"^
+ 0(4)=A+4B + 16C + 64D + 256E+ .... +4"K. "
Therefore 0=0+0 + 0 + 0 + 24E+PF+ .... +TK.
Hence E = F= . . . . K = 0, and therefore 0(«) must be afnnc^
tion of the third degree in order that the prismoidal formula uisy
apply. j
§ 107. If we take (p{x) = A + Bx + Ck" + Dx», there will be as many
possible varieties as there are combinations of four things, one, twoj
three, apd four together, i.e., 2*- 1 = 15 varieties. Corresponding
to each of these there will be ai least one solid the area of a section
of which at a distance x from one of the parallel planes is
0(x)=A + Ba:+Car'+Dii:^, and at least one solid of revolution
generated by the curve whose equation is of the form -
«^=0(x)»A + Bx+Ca^+Dx».
As space prevents us discussing all the cases that may arise, ;va.
content ourselves by giving three examples as illustrations.
(a) Volume of an ellipsoid. — Here 0(x) = Bx + Cx-.
Let 2a, 2b, and 2c be the axes of wiiich 2a is the greatest, theni
A«=2a, Ai=0i, A3=0, and A.=Trbc ;
therefore volume = iA(A, + 4Aj + A3) = la{iirbc) = f iroJc , •
which agrees with the result in § 104.
(/9) Vohcme of a sphere. — Here jr!/-=0{x) = Ba!+Cx'.
Let r be the radius of the sphere, then ft=2r, A,=0, A]— 0, ao^
A,=jrr', hence, as before (§ 91),
volume of sphere = iA(Ai+4Aj+ A3)=^(4Tr')=|«J.'',
(■y) Volume of a right circular cone. — Here iri/'=0(x) = Cx'.^
Let r=radius of base and h the altitude, then Aj = 0, A,"-«r*,'
and A3=ir(Jr)2 ; hence ~''
volume of cone = J7i {Ai + 4A3 + A3 }= Jft {irT* + ipr" } = JAw"
In a similar manner we can determine the volumes of a cylindeTy',
a prolate spheroid, an oblate spheroid, &c.
§ 108. In general, if in any solid we have
0(x) = A + Bx + Cx^ + Da» ,
where A, B, C, and D are known constants, then, if A be the IeDj;t]t
of the solid,
Ai-0(O)=A,
A. - 0(P) = A + B(4A) + C(iA)» + D(iA)» ,)
A3=0(A)-A + BA + CA2 + DA\
and therefore
volume of solid ■=}A(A, + 4A, + A3)
= AA + 4B A- + JCA' + iDft* .
I. Solids of Revolution in General.'
§ 109. Volume of any Solid of Revolution. — Lei P,P, . . ','7 PiJ
(fig. 84) be the generating curve, and A, . . . . A„ the axis of
revolution. Divide the curve into portions in the points P., Pj,
&c., and ditiw the chords and tangents of the small arcs PiP),
P3P3, &c. , then it is evident that the solid generated by the curve
is greater than the sum of the conical frusta traced out by the
chords and less than the sum of the conical frusta traced out by tho
tangents. Hence, by increasing the number of chords, namely, by
increasing the points of division of the curve, we can make the
difference between these sums as small as we please, and therefore
by this method we can approximate as closely as we please to the
volume of the solid generated. |
Assuming that the points P,, Pj, P3 arc so near each other that
the solid generated differs little from the fmstum of a cone, andl
using the same notation as in § 63, we have volume generated by
P,PsPj=}7rA,A,(s; + 4s! + s:)- Js2A,A,(«J + «J + »y
-» Jiro(s; + 45^+»j) J
similarly the volume generated by
P3P4P5 = Jira(s5 + 4«; + sj) ;
whence the volume generated by the whole curve PiPj . . . . P« ^^
-iia{»;+4+2(^+s:+ .... +sii-8)+4(s;+«:+ . . • ■ +^-i)}»,
'28
M E N — M E N
. &c.)
l—j^{cl+e^ + 2{cl + el+ +el.i) + 4{cl + cl+ +cl.-i)},
[« formula more convenient m practice, as it is sometimes more easy
ito measure equidistant circumferences than equidistant radii.
J. TTieorcms of Pappus.
§ 110. The following general propositions concerning surfaces and
soUds of revolution, usually called Guldiu's theorems, are worth the
reader's attention.
If any plane curve revolve about any e::temal axis situated in its
plane, then
(a) the surface of the solid which is thereby f^enerated is equal
to the product of the perimeter of the revolving curve and the
'length of the path described by the centre of gravity of that peri-
meter ;
(/3) the volume of the solid is equal to the product of the area of
the revolvin;^ curve and the length of the path described by the
centre of gravity of the revolving area.
We content ourselves with an example or two of the application
of these theorems, referring to the article Infinitesimal Calculus
for the proofs.
Example 1. — To find the surface and volume of a circular ring. —
Let a be the distance of the centre of the generating curve, in this
case a circle, from the axis of rotation, and r the radius of the
circle, then ^
perimeter of generating curve = 2irr ,
area of generating curve = irr^, and
path described by the centre of gravity either of the perimeter oi*
area = 2Tra: hence
surface of ring = 27rr x 2jra = 4jrra, and
volume of ring = Trr^ x 2»ra = 27r7^a.
Example 2. — To find the volume swept out by an ellipse wnose
Axes are 2a and 2i, revolving about an axis in its own plane whose
liistance from the centre of the ellipse is c.
Here area of generating cui-ve =7r«6,
Uld path described by centre of gravity Oi area —2tc ; hence
volume generated = 7ra6 x 2TTC=2Trabc.
ICxample 3. — A circle of r inches radius, with an inscribed regular
hexagon, revolves about an axis a inches distant from its centre, and
parallel to a aide of the hexagon ; to find the diHerence in area of
the generated surfaces and volumes.
Here perimeter of circle =■ Sttt ,
and perimeter of hexagon = 12 xrsin 30" (§ 17)
also area of circle = irr^,
and area of hexagon = 3r2sin60*' (§ 18, $)
«-|V3r2;
hence difference of surfaces generated
== iirra - 1 2iTar = iirar(Tr - 3) ;
and difference of volumes generated
= 2ir'j-a - 37rr2v'3/i
= 3rr^a(27r-3V3).
I PART III. GAUGING.
5 111. By gauging is meant the art of measuring the volume of a
cask, or any portion of it. The subject is one of great interest and
practical importance, but space will only permit us to discuss it very
1>riefly. If the cask whose capacity we wish to determine be a solid
of revolution, then its volume can at once bo computed, either
exactly or approximately, by the methods already descrilied.
It is usual to divide casks into the following four Classes according!
to the nature of the revohing curve : — -^
(a) the middle frustum of a spheroid ,
(^) the middle frustum of a parabolic spindle ;
(7) two equal frusta of a paraboloid, united at their bases j'
(5) two equal frusta of a cone, united at their bases.
Casks of the second, third, and fourth variety are rarely met withH
in practice, and we shall accordingly confine our attention to th©!
first kind, which is considered the true or model form of cask. 4
Let ABCD (fig. 5G) be a section of the cask, and assume it to bo'
the middle frustum of a prolate spheroid, then
its volume = ^7r(2i- + 6;)^ ,
where A=OT, h^=AX, and fc=X5' {§ 99).
YY' is called the bung diameter, and AB or CD the head]
diameter.
An imperial gallon contains 277 '274 cnbic inches, and tierefor©
the number of gallons in the above cask
tr{2b"' + b])k
"'3x277*274"831-822''
J2d^-\,
V 1059-1 y
2(252+6;)^
, where d = 2h, dj==2bi;
-to the square of the head diametef
_ diameter, m
; by ;
whence we have the rule :
add twice the square of the bung diameter, multiply the sum by Iho'
length and divide the result by 1059 '1, and the answer is the con-:
tent in imperial gallons.
Casks as ordinarily met with are not true spheroidal frusta, bat
it is better to consider them as
such, calculate their capacity on
this assumption, and then make
allowance for the departure from
the spheroidal form. The de-
termination of the properallowance-
to be made in each case is a matter
depending on the skill and ex-
perience of the gauger, and pro-
ficiency in the art can only be
attained by considerable practice.
§ 112. If the cask be very little "
curved, wo obtain au approxima- ^^'
tion to itg capacity by considering it as made up of two equal.fnista
of a cone, united at their bases. Hence from § 83 we have
volume of cask= ijr?i{rl + TiT^ + tD nearly.
Hero we neglect the small volumes generated by APY. YSu,
BQY', and Y'RC ; and therefore the volume is too small.
If we put r^r^ = r\ we obtain
volume = y:h{2r\ + t\) ,
which is a little too large, and therefore the true volume lies between
these two limits, and a very close iiDDroximation to it is said to be
given by the formula
% 113. Ullage of a Cash. — The quantity of liquor contained in a
cask partially tilled and the capacity of the portion which is empty,
are termed respectively the wet and dry ullage.
(a) Ullage of a standing cask. — By mean'-' of the method applied
in § 105, the following rule is deduced : —
Add the square of the diameter at the surface, the square of the
diameter at tlie nearest end, and the square of double the diameter
half-way between ; multijily the sum by the length between the
surface and the nearest end, and by '000472.
The product will be the wet or dry ullage according as the lesser
portion of the cask is filled or empty.
(jS) Ullage of a lying cask. — The ullage in ^ms case is found
approximately on the assumption that it is proportional to the seg-^
meut of the bung circle cut off by the surface of the liquor. The
rule adopted in practice is
ullage= 5 content x segmental area. (W. T.*)
MENTAL DISEASES. See Insantty.
MENTON (Ital., Mentone), a cantonal capital in the
'department of Alpes-Maritimes, France, situated 15 miles
north-east of Nice, on the shores of the Mediterranean,
The town, which has a pojiulation of about 8000, rises
like an amphitheatre on a promontory by which its semi-
circular bay (5 miles wide at its entrance, and bounded on
the W. by Cape Martin and on the E. by the chffs of La
iMurtola) is divided. It is composed of two very distinct
[portions . below, along the sca-shorc, is the town of hotels
and of foreigners, which alone is accessible to^wheeled,
vehicles ; above is that of the native Mentonese, with]
steep, narrow, and dark streets, spread over and clinging
to the mountain, around the strong castle which was once
its protection against the iattacks of pirates. Facing the
south-east, and sheltered on the north and west by higW
mountains, the Bay of Mcnton enjoys a delicious chmateJ
and is on this account much frequented by invalids rej
quiring a mild and equable temperature. The mean foij
the year is Gl° Falir.. exceeding that o£ Rome or 05
M E N — M E R
29
^i^ and "equalling that of Naples. Frost occura on
the average only once in ten years ; in one particular
[year the thermometer did not fall below 46° Fahr. In
bummer the heat is never very great, the temperature
'rarely exceeding 86° Fahr. Winter and summer are the
imost agreeable seasons; in autumn the rain storms are
accompanied by sudden changes of temperature, and in
spring the sea breezes are apt to be violent. Besides the
charms of its climate, Menton offers those of an almost
tropical vegetation. Lemon-trees, olive-trees, and pines,
rising above each other in successive stages, adorn the sur-
rounding slopes. The district produces forty millions of
lemons yearly, and this is the principal source -of its natural
wealth. The olive-trees are remarkable for the great size
they have attained in the course of the centuries during
which they have continued to bear. Of their wood a
multitude of fancy objects are made for sale to strangers.
The origin of Menton is unknown. During the Middle Ages it
was successively occupied by llic .Saracens, the Genoese, and the
princes of Anjou. In the middle of the 14th centui'y it was pur-
chased as a single domain by tiie Grimaldis, lords of Monaco.
Daring the times of the republic and the first empire it belonged
to France ; but in 1815 it ngain became the property of the
princes of Monaco, who subjected it to such exactions that in 1848
Its inhabitants, weary of finding their reasonable demands put off
with empty promises, proclaimed their town free and independent,
under the protection of Sardinia. Menton, with the neighbouring
commune of Roquebrune, was united to France in 1860, at the same
kime as Nice and Savoy.
MENTZ. See Mainz.
MENZEL, Wolfgang (1798-1873), poei, critic, and
liistorian, was born June 21, 1798, at Waldenburg in
Bilesia, studied at Breslau, Jena, and Bonn, and after
living for some time in Aarau and Heidelberg finally
settled in Stuttgart, where, from 1830 to 1838, he had a
^eat in the Wiirtemberg "landtag." His first work, a
tiever and original volume of poems, entitled Slrechverse
(Heidelberg, 1823), was followed in 1824-25 by a popular
Geschichie der Deutschen in three volumes, and in 1829
and 1830 by Jiubezahl and Jfarciisus, the ballads upon
which his reputation as a poet chiefly rests. In 1851 he
published the romance of Furore, a lively picture of the
period of the Thirty Years' War ; his other very numerous
writings include Geschichie Europa's, 1789-1815 (1853),
and histories of the German war of 1866 and of the
Franco-German war of 1870-71. From 1825 to 1848
Menzel edited a " Literaturblatt " in connexion with the
Morgenblatt ; in the latter year he transferred his allegiance
from the Liberal to the Conservative party, and in 1852
his " Literaturblatt " was again revived in that interest.
In 1866 his political sympathies again changed, and alibis
energies were employed to oppose the " particularism " of
the Prussian "junkers" and the antiunionism of South
Germany. He died on April 23, 1873. His large private
library of 18,000 volumes was afterwards acquired for the
university of Strasburg.
MEPHISTOPHELES, the name of onu of the personi-
fications of the principle of evil. In old popular books
and puppet-plays the word appears in various forms, —
as Mephistophele's, Mephistophiles, Mephistophilis, and
Mephostophilis. In the Tragical History of Doctor
Faustus, Marlowe writes "Mephistophilis"; in the Merry
Wives of Windsor we find " Mcphistophilus." The etymo-
logy of the word ia uncertain. According to one theory,
it may be taken to represent /itjc^uotoi^iAtj? ; in which case
the meaning would be " one who loves not light." Another
theory is that the word is a combination of the Latin
"mephitis" and the Greek <^i\o9, signifying "one who
loves noxious exhalations." Probably it is of Hebrew
origin, — from 15*?, a destroyer, and 7^^, taken to mean a
liar. ^ This view is supported by the fact that almost all
the names of devils in the magic-books of the 16th century
spring from the Hebrew. In the old Faust legends the
character of Mcphistopheles is simply that of a powerful
and wicked being who fulfils Faust's commands in order to
obtain possession of his soul. Marlowe attributes to him
a certain dignity and sadness, and there can be little doubt
that the Mephistophilis of the Tragical History suggested
some important traits of Milton's Satan. The name has
been made famous chiefly by Goethe, whose conception of
theicharacter varied at different perjods of his career. Ia
the fragment of Faust published in 1790, but written
many years before, Mcphistopheles has a clearly marked
individuality; he is cynical and materialistic, but has a.
man's delight in activity and adventure, and his magical
feats alone remind us that he is preternatural. In revising
and extending this fragment, which forms the chief portion
of the first part of Faust, Goethe treated Mephistopheles
as the representative of the evil tendencies of nature,
especially of the tendency to denial for its own sake, rather
than as a living person. This character Mephistopheles
maintains in the second part, where, indeed, the name often
stands for a pure abstraction.
See Julius Mosen, Faust ; Diintzer, ErlHuterungm, BU Ooethe'i
JVerken : Faiist ; Vischer, Goethe's Faust.
MEQUINEZ (the Spanish form of the Arabic Mihndsa),
a town of Morocco, the ordinary residence of the emperor,
is situated in a fine hilly country about 70 miles from the^
west coast and 35 west-south-west of Fez on the road to
Bailee, in 34° N. lat. and 5° 35' W. long. The town-wall,
with its four-cornered towers, is kept in good condition;
and a lower wall of wider circuit protects the luxuriant
gardens with which the outskirts are embellished. In the
general regularity of its streets, and in the fairly substantial
character of its houses, Mequinez ranks higher than any
other town in Morocco ; but it possesses few buUdings of
any note, except the palace, and the mosque of Mulei Ismael,
which serves as the royal burying-place. At one time the
palace (founded in 1634) was an imposing structure, but
the finest part has been allowed to go to ruin. In 1721
Windhus described it as " about 4 miles in circumference,
the whole building exceeding massy, and the walls in every
part very thick ; the outward one about a mile long and 25
feet thick." The best part consisted of oblongs enclosing
large open courts or gardens. Mortar or concrete was t^-o
principal material used for the walls, but the pillars v.-ere
in many cases onarble blocks of. great beauty and costliness
(A Journey to Mequinez, London, 1725). Most of the
inhabitants of Mequinez are connected more or less directly
with the court. Their number has been very variously
estimated by different travellers. Graberg de Hemso gives
56,000 in 1834, Eohlfs in 1861 from 40,000 to 50,000,
and Conring in 1880 about 30,000. The town was
formerly called TAkarart. . Edrisi refers the present name
to a Berber chief MeknAs. ^
MERAN, a favourite health resort, and the capital of »
district in South Tyrol, Austria, is pictiu'esquely situated
at the foot of the vine-clad Kiichelberg, on the right bank
of the Passer, about half a mile above its junction with the
Adige, and 45 miles to the south of Innsbruck. Meran'
proper consists mainly of one long narrow street, called
the Laubengasse, flanked by covered arcades. In a wider
sense, the name is often used to include the adjacent
viUages of Untermais, Obermais, and Gratsch. The most
noteworthy buildings are the Gothic church of St Nicholas,'
with its lofty tower, dating from the 14th and 15th
centuries; the Spitalkirche, built in the 15th century, and
restored in 1880; and the quaint old Fiirstenhans, or
residence of the counts of Tyrol. The town contaii.s a
gymnasium, a nunnery and school for girls, an institution'
for sick priests, and several other charitable establishments.!
.30
M E il ~ M E R
MBran owes lis liigh reputation as a resort for consumptive
and nervous invalids to the purity ' of its air and its com-
parative immunity from wind and rain in winter. It stands
in 46° 41' N. lat., at^a height of 1050 feet above the sea,
and has a mean annual temperature of about 54° Fahr.
Meran enjoys three seasons, being also visited in spring
for the whey-cure and in autumn for the grape-cure. The
arrangements for the comfort of the visitors are very com-
plete; and the environs afford opportunity for numerous
pleasant walks and excursions. The favourite promenade of
the inhabitants is on a massive dyke, built to protect the
town afjainst the encroachments of the Passer. Nearly
twenty old castles and chateaus are visible from the bridge
over the Passer, the most interesting being Schloss Tyrol,
an ancient edifice which has given its name to the entire
country. Meran is now frequented by about 6500 patients
and 8000 to 9000 passing travellers annually. In 1880 its
population, including Obermais and Untermais, amounted
to 5334 souls.
Meran is probably the representative of the Boman CTrbs Majeiisis,
afterwards known as Mairania. It became a town in 1290, and
down to 1490 was the capital of the counts and dukes of Tyrol.
The town suffered somewhat during the Peasants* War in the 16th
centiu-y, and subsequently from destructive Hoods. As a health-
resort it has been known for about forty years. The whole region
in which it lies is singularly rich in historic interest
Aulhoritifs.—Beda Weber, Meran-, Dliringsfeld, Aui Meran, 1808; Noe, Der
FruhUng von Meran ; Stampfev, Clironik ion Meran, 18U7. and Oeschichto der
Stadt Meran, 1872 ; Piiclier, Meran ah Ktimatiseher Kurort, 1870 ; Plaot. Fiihrer
diu'Ch Meran, 2d ed., 1879 ; Knoblauch, Meran, 5th ed., 1881
MERCATOR, Geeakdus (Latinized form of Gerhard
Kramer) (1512-1594), mathematician and geographer, was
bom at Rupelmonde in Flanders, May 5, 1512. Hav-
ing completed his studies at Louvain, he devoted him-
self to geography, and, after being for some time attached
to the household of Charles V., he was appointed cosmo-
grapher to the duke of Juliers and Cleves in 1559, taking
up his residence at Duisburg, where he died December 2,
1594. One of his earliest cartographical works was a
terrestrial globe (1541), followed in 1551 by a celestial
globe. In 1552 he published a treatise De tisu annuH
ditronomici (Louvain), and at Cologne in 1569 his Clirono-
logia, hoc est Umporum demonsiratio . . . ab initio mundi
usque ad Anmim Domini 1568, ex eclipsibiis et observa-
tionibus astronomicis, sacris quoque Sibliis, &c. In the same
year was published the first map on Mercator's well-kno^^'n
projection, with the parallels and meridians at right angles,
for use in navigation. At Cologne, in 1578, appeared his
Tabulx geographicee ad mentem Fiolemsei reslitutse et.emend-
<Ux. The work by which he is chiefly known is his atlas,
published in 1594 at Duisburg, in folio, under the title of
Atlas, sive Cosmographica; medilationes de fabrica mundi.
It contains, besides the maps, cosmographical and other
dissertations, some of the theological views in which were
condemned as heretical ; it was completed by Hondius in
1607. Several of the maps had been previously published
separately, the atlas being dehvyed to allow Ortelius to
complete his. Mercator also oublished in 1592 a Jlar-
monia Evangeliorum.
\ MERCURIAL AIR-PUMP. This name is given to
two distinct instruments, one of which is founded on
statical, the other on hydrodynamica! principles.
1. The Statical Pump. — The famous spiritualist Sweden-
borg was the first to conceive an air-pump in which a mass
of mercury, by being made to rise and fall alternately
within a vertical vessel, should do the work which in the
ordinary instrument is assigned to the piston. Ho pub-
lished a description of his pump in 1722; but it is
questionable whether his design was ever realized. Of
numerous subsequent inventions the only one which, in
fact, has survived is the admirably simple and yet efficient
instroment first described in 1858, but constructed some
Fio. 1. — Geisler'e
Mercurial Air- Pump.
time before, by H. Gei.'Jer of Bonn, w'lich at once, and"
justly, met with universal acceptance.
The general scheme of Geisler's pump is shown in fig. 1.'
A and B are pear-shaped glass vessels connected by a long
narrow indiarrubber tube, which must
be sufficiently strong in the body (or
strengthened by a linen coating) to
stand an outward pressure of 1 to L}
atmospheres. A terminates below in a
narrow vertical tube c, which is a few
inches longer tlian the height of the \
barometer, and to the lower end of this
tube the india-rubber tube is attached
wliich connects A with B. To the
upper end of A is soldered a glass two-
way stop-cock, by turning which the
vessel A can either be made to com-
municate through s and a hole in the
hollow cock with the vessel to be ex-
hausted (I._, fig. 2), or through g with
the atmosphere (II., fig. 2), or can be
shut off from both when the cock holds
an intermediate position. The apparatus,
after having been carefully cleaned and
dried, is charged with pure and dry mer-
cury, which must next be worked back-
wards and forwards between A and B to
remove all the air-bells. The air is then driven out of A by
lifting B to a sufficient level, turning the cock into position
n., and letting the mercury flow into A untU it gets to
the other side of the stop-cock, which is then pkiced in
the intermediate posi-
tion. Supposing the
vessel to be exhausted
to have already been
securely connected with
b, we now lower the
reservoir B so as to re-
duce the pressure in A
sufficiently below the
tension in the gas to
be sucked in, and, by
turning the cock into
position I., cause the gas
to expand into and al-
most fill A. The cock
is now shut against both
a and b, the reservoir
lifted, the gas contents
of A discharged through
a, and so on, untU, when
after an exhaustion mer-
cury is let into A, the
-Arrangements of Stoo-Cock
in Air-Pump.
metal strikes against the top without interposition of a
gas-bell. In a well-made apparatus the pressure in tha
exhausted vessel is now reduced to y^ or ^ of a milli-
metre, or even less. An absolute vacuum cannot be pro-
duced on account of the unavoidable air-film between the
mercury and the walls of the apparatus.
Tlie great advantage of the mercurial over the ordinary air-pump
is tliat it evacuates far more completely than the latter, that it
nffrrds direct and unmistakable evidence of the exhaustiveness of
its work, and — last not least — that it enables one to transfer thegsa
sucked out to another vessel without loss or contimination, so that
it can be measured and analysed. On account of this latter feature
ruoro especially, the instrument is highly valued as an auxiliary in
gasometric researches. Without it the researches on which rests
our present knowledge of the gases of the blood could not have been
I carried out. The actual instrument, as constructed for various
I kinds of work, has of course various complexities of detail omitted
in tho above description. For these the reader must refer to hand;'
boolm of practical physiology.
]M E R — M E R
31
As it takes a height of abont 30 inches of mercury to balance
[the pressure of the atmosphere, a Geisler pump necessarily is a
tomewhat long-legged and unwieldy instrument. It can be con-
nderably shortened, the two vessels A and B broudit more closely
together, and the somewhat objectionitilo india-rubber tube be dis-
pensed with, it we couuect the air-space in B with an ordinary air-
j'Ump, and by means of it do the greater part of the sucki]ig and
|the whole of the lifting work. An instrument thus modified was
coDstructed by Poggendorff (see his Annalcn, vol. cxxv. p. 151,
1865), and another, on somewhat different principles, by Prof.
Dittniar (see the " QMllcngcr " Reports).
Even a Geisler's stop-cock requires to be lubricatea to be abso-
lutely gas-tight, and this occasionally proves a nuisance. Hence a
number of attempts have been made to do witliout stop-cocks alto-
gether. In Topler's pump' this is attained by using both for tlie
inlet and the outlet vertical capillary glass'tubes, soldered, the
former to Somewhere near the bottom, the latter to the top of the
vessel. These tubes, being more than 30 inches high, obviously
act as efficient mercury-traps ; but the .already considerable height
of the pump is thus multiplied by two. This consideration has led
Alexander Mitscherlicli (Pogg. Ann., cl. 420, 1873), and quite
lately F. Ncisen (Z. f. Inslrummicnkunde, 1882, p. 285) to intro-
duce glass valves in lieu of stop-cocks. As glass floats on mercury,
such valves do not necessarily detract from the exhaustive power
of the pump.
2. The Dynamv: Pump. — This was invented in 1865 by
H. SprengeL The instrument, in its original (simplest)
form (fig. 3),. consists of a vertical
capillary glass tube a of about
1 mm. bore, provided with a
lateral branch 6 near its upper
end, which latter, by an india-
rubber joint governable by a screw-
clamp, communicates with a funnel.
The lower end is bent into the
Flo. 3. — SprengeL'a
Air-Pump.
shape of a hook, and dips into a
pneumatic trough. The vessel to
be exhausted is attached to b, and,
ip order to extract its gas contents,
a properly regulated stream of mer-
cury is allowed to fall through the
vertical tube. Every drop of mer-
ciuy, as it enters from the funnel,
entirely closes the narrow tube like
a piston, and in going past the
place where the side tube enters
entraps a portion of air and carries
it down to the trough, where it can
be collected. If the vertical tube,
measuring from the point where
the branch comes in, is a few inches
greater than the height of the
barometer, and the glass and mer-
cury are perfectly clean, the apparatus slowly but surely
produces an almost absolute vacuum.
■ The great advantages of Sprengel's pump lie in the simplicity of
its construction and in the readijiess with which it adapts itself to
the collecting of the gas. It did excellent service in the hands of
Graham for the extraction of gases occluded in metals, and since
then has become very popular in g.is-laboratories, especially in
Britain. Many improvements upon the original construction have
been proposed. One of these which deserves mention is to pass the
mercury, before it enters the " falling " tube, through a bulb in
which a good vacuum is maintained, by means of an ordinary air-
pump or a second "Sprengel." (\V. D.)
MERCURY was the Roman goa who presided over
barter, trade, and all commercial dealings. His nature is
probably more intelligible and simple than that of any
other Roman deity. His very name, which is connected
with TTurx, mercator, kc, shows that he is the god of
merchandise and the patron of merchants. In the native
Italian states no merchants and no trade existed till the
.influence of the Greek colonies on the coast introduced
Greek customs into the cities of the land. All the usages
r ' See Dingler's Polytechn. Journal, 1862 ; an imnroved form by
S?8sel-Qagen is described in Wiedemann'a AnntUen, iii. 425, 1881.
and terminology of trade, and all the religious ceremonies
conjiected with it, were borrowed by the Romans from the
Greeks. It was no doubt under, the rule of the Tarquiiis,
when the prosperity of the state and its intercourse with
the outer world were so much increased, that merchanU
began to ply their trade in Rome. Doubtless the
merchants practised their religious ceremonies from the
first, but their god filercuiius was not ofiiciaUy recognized
by the state till the year 495 b.c. Rome frequently suffered
from scarcity of corn during the unsettled times that
followed the expulsion of the Tarquins. Various religions
innovations were made to propitiate the gods ; in 496 the
Greek worship of Demcter, Dionysus, and Persephone
was established in the city (see Liber), and in 495 the
Greek god Heemes (q.v.) was introduced into Rome under
the Italian name of Mercurius (Livj', ii. 21, 27). Preller
thinks that at the same time the trade in corn was rcu-
lated by law, and a regular college of merchants was
instituted. This collegium was under the protection of the
god ; their annual festival was on the Ides of May, on
which day the temple of the god had been dedicated at
the southern end of the circus maximm, near the Aventine •
and the members were called mercurinles as well as
mercatores. The Ides of May was chosen as the feast of
Mercury, obviously because Maia was the' mother of
Hermes, i.e., of Mercury (see Maia) ; and she was wor-
shipped along with her son by the mercurinles on this
day. According to Preller, this religious foundation had
a political object ; it established on a legitimate and sure
basis the trade between Rome and the Greek colonies of
the coast, whereas formerly this trade had been e-Tposed to
the capricious interference of the Government officials for
the year. Like all borrowed religions in Rome, it must
have retained the rites and the terminology of its Greek'
original (Festus, p. 257). Mercury became the god, not
only of the mercatores and of the corn trade, but of buying
and selling in general ; and it appears that, at least in the
streets where shops were common, little chapels and images
of the god were erect yj. There was a spring dedicated to
Mercury between his temple and the Porta Capena ; every
shopman drew water from this spring on the Ides of May,'
and sprinkled it with a laurel twig over his head and over
his goods, at the same time entreating Mercury to remove
from his head and his goods the guilt of all his deceits
(Ovid, Fasti, v. 673 sq.). The art of the Roman tradesmad
was evidently like that of an Oriental tradesman in modern
times, and the word mcrcurialis was popularly used as
equivalent to " cheat." In the Latin poets Mercury is often:
gifted with some of the manifold characters of the Greek'
Hermes, but this finer conception seems to have had no'
real existence in Roman religion.
Roman statuettes of bronze, in which Mercury is represented, like
the Greek Hermes, standing holding the caduceus in the one hand
and a purse in the othei-, are exceedinely common. The caduceus
rnust have been introduced as a symbol of Mercury at a very early
time, for it is found on Italian coins as early as tlie 4th century
before Christ, and we learn that several were kept.as sacred objects
in the adytumol the sanctu.iry at Lavinium (Dion. Hal., i. 67).
But its foreign origin is shown by the fact that, although it was s
sign of peace, it was never borne by the fdialcs, the old Italino
heralds. The very name is derived from the Greek Kvpixeioy.
Preller's view (iJtIm. Myth.) that mercuriahs and mercatores are
the same guild is a tempting one. but its truth is very doubtfuJL;
Mommsen thinks that mercurialcs were a purely local guild, viz.,
the pagani of the Circus valley.
MERCURY, in chemistry, is a metal (symbol Hg) which
is easily distinguished from all others by its being liquid
at even the lowest temperatiu-es naturally occurring in
moderate climates. To this exceptional property it owes
the .synonyms of quicksilver in English (with the Germans
quecksilber is the only recognised name) and of hydrar-
gyrum (from uSiDo. water, and dfyyupoi, silver) in Gr>eco-Latin.
S2
MERCURY
?rhis metal does not api)ear to have been Icnown to the
ancient Jews, nor is it mentioned by the earlier Greek
.•writers. Theophrastus (about 300 B.C.) mentions it as a
derivative of cinnabar. With the alchemists it was a
substance of great consequence. Being ignorant of its
susceptibility of freezing into a compact solid, they did not
recognize it as a true metal, and yet, on the authority of
Gober, they held that mercury (meaning the predominating
element in this metal) enters into the composition of all
metals, and is the very cause of their metaUicity. When,
about the beginning of the IGth century, chemistry and
scientific medicine came to merge into one, this same
mysterious element of " mercury " played a great part in
rthe theories of pathology ; and the metal, in the free as in
,certain combined states, came to be looked upon as a
ipowerful medicinal agent, which position, on purely em-
Ipirical ground.s, it continues to bold to the present day.
Mercury occurs in nature chiefly in the form of a red
sulphide, HgS, called cinnabar, which, as a rule, is accom-
panied by more or less of the reguline metal, — the latter
being probably derived from the former by some secondary
reaction. The most important mercury mines in Europe
are those of Almaden in Spain and of Idria in Illyria ;
these until lately furnished the bulk of the mercury of
commerce, but they are now almost ecUpsed by the rich
deposits of New Almaden in California. Considerable
quantities of mercury are said to be produced in China and
in Japan ; minor deposits are being worked in the Bavarian
Palatinate, in Hungary, Transylvania, Bohemia, and Peru.
At Almaden the ore forms mighty veins traversing micaceous
schists of the older transition jieriod ; in IlljTia it is dis-
seminated in beds of bituminous schists or compact lime-
[stone of more recent date.
Chemically speaking, the extraction of merciu'y from its
tores is a simple matter. Metallic mercury is easily vola-
tilized, and separated from the gangue, at temperatures far
below redness, and cinnabar at a red heat is readily reduced
po the metallic state by the action of iron or Ume or
atmo.spheric oxygen, the sulphur being eliminated, in the
first case as sulphide of iron, in the second as sulphide
and sulphate of calcium, in the third as sulphurous acid
■gas. To the chemical mind a close iron retort would
suggest itself as the proper kind of apparatus for carrying
out these operations, but this idea is acted upon only in
a few small establishments, — for instance, in that of Zwei-
briicken in the Palatinate, where lime is used as a decom-
posing agent. In all the large works the decomposition
of the cinnabar is effected by the direct exposure of the
ore to the oxidizing flame of a furnace, and the mercury
[vapour, which of course gets diffused through an immense
mass of combustion gases, is sought to be recovered in
jnore or less imperfect condensers.
^ At Alnmden this roasting distillation is effected in prismatic
furnaces, which, by a second upper (brick) grating are divided into
Itwo Oats, tlio lower one serving for tlie generation of a wood iire,
■while the upper accommodates tlie ore, wliicli is inti-oduced through
nn opening in tlie dome-shaped roof. To avoid au excessive diiu-
;tion of tlie mercury vapour witli coinhustion gases, pait of these are
iled out laterally into a chimney and the rest allowed to strike up
(through the heap of ore. The large mass of metalliferous vapour
■produced passi'S out through a system of pipes inserted laterally into
tlie dome and so ari-auged that they follow tirst a descending and
,tlien an ascending iilaiic, to lead ultimalely into a condensation
chamber which communicates in its turn with a chimney. Tlie
,pipes are formed each of a largo number of elongated pear-shaped
earthenware adapters (called aliulch), which are telescoped into
one another as in the rase of the iodine-distillation ajiparatus, the
lioints being luted with clay. The lowest row of aludels, wliicli
Ilie in the line of intersection of the two inclined planes, are pierced
with holes below, so that what arrives as liiiuid mercury there
i-uns out into a gutter leading to a reservoir. Wliat of mercury
vapour remains uncondensed in the aludels passes into the chamber,
the intention being to have it condensed there ; in reality a large
jiroportiou of_tho mercury passes out thr'ough the chimney (and
through the numerous leaks in the aludels) into the atmosphere'
to poison the surrounding vegetation and the workmen. Similar
furnaces to the Almaden ones are used in Idiia and at Now
Almaden ; only the conden.sation apparatus are a little less im-
perfect. But in all three places the loss of metal is very consider-
able ; at New Almaden it is said to amount to close upon 40 per cent
The mercury obtained is purified mechanically by straining it
through dense linen bags, and then sent out into commerce in leather
bags, or iu wrought-iron bottles provided with screw plugs, each
J'olding about 75 It* avoirdupois.
According to BalHng's Metallurgische Chemie (Bonn,-
1882), the production of mercury in the years named was
as follows : —
Austria, exclusive of Hungary (1880) 369 tons.
Hungary (1879) 180 „
Italy (1877) S5 „
Spain (1873) 929 „
United States (1875) '2054 „
Assuming the amount to be the same from year to year,
this gives a total of 3587 tons.
The price of the metal is subject to immense fluctuations ;]
it generally ranges from 2s. to 7s. Cd. a pound avoirdupois.'
Commercial mercury, as a rule, is very pure chemically,'
so that it needs only to be forced through chamois leather
to become fit for all ordinary applications ; but the metal,!
having the power of dissolving most ordinary other metals,'
is very liable to get contaminated with these in the labora-'
tory or workshop, and requires then to be purified. For
this purpose a great many chemical methods have been'
proposed, which, however, all come to this, that the
base admixtures are sought to be removed by treatment
with nitric acid, oil of vitriol, or other agents which act
preferably on the impurities. The best of these methods
is that of Briihl, who shakes the metal with a solution of
5 grammes of bichromate of potash and a few cubic centi-
metres of sulphvu-ic acid in one litre of water, until the red
chromate of mercury, first produced, has disappeared, and
its place been taken by green chromic sulphates. The
supernatant liquor and chromic scum are washed away by
a powerful jet of water, and the clean metal is dried and
filtered through a perforated paper filter. The only really
exhaustive method is redistillation out of a glass apparatus.
Unfortunately the operation is difficult of execution, as
mercury " bumps " badly on boihng ; but this can be
"avoided by distilling the metal in a jKrfect vacuum. An
ingenious apparatus for this purpose, in which the distilled'
metal itself is made to keep up the vacuum, was con-
structed lately by Leonhard Weber. A U-tube, the limbs
of which are longer than the height of the barometer, is
filled with pure mercury, and inverted, the one Uinb
being made to dip into a vessel with pure, the other
into another containing the impure, mercury. This second
limb is inflated above so that the meniscus is about the
middle of the bulb. This bulb is heated, and the conse-
quence is that the metal there distds over into the first
limb to add to the supply of pure metal, the impure
rising up in the second by itself ;o maintain a constant
level. Dewar has modified the apparatus so that there
is no need of a supply of pure metal to start with.
Absolutely pure mercury docs not at all adhere to any
surface which does not consist of a metal soluble in mercury.
Hence the least quantity of it, when placed on a sheet of
paper, forms a neatly rounded-off globule, which retains its
form on being rolled about, and, when subdivided, breaks
up into a number of equally perfect globules. The presence
in it of the minutest trace of lead or tin causes it to " draw
tails." A very impiu'e metal may adhere even to glass,'
and in a glass vessel, instead of the normal convex, form
an irregular flat meniscus.
Properlies. — The pure metal is silver-white, and retains
its strong lustre even on long exposure to ordinary air.
At - 38°-8 C, i.e., - 37°-9 F. (Balfour Stewart), it freezes,
MERCURY
33
with considerable contraction, into a compact mass of
r^nlar octahedia, which can be cut with a knife and be
flattened under the hammer. The specific gravity of the
frozen metal ja 14'39 ; that of the liquid metal at 0° C. is
13-595 (water of i' C. ■= 1). Under 760 mm. pressure
it boils at 357'-3 C. (675'-l Fahr.) (Regnault). At very
low temperatures it seems to be absolutely devoid of
Tolatility (Faraday); but from - 13' C. upwards (Regnault)
it exhibits an appreciable vapour tension.
The following table gives the tensions "p," in millimetres
of mercury of 0° C, for a series of centigrade temperatures
"t," according to EegnauU : —
t- 0' 10' 20° 60° 100° 150° 200°
/>--02 -OS -04 -11 75 4-27 19 90
t- 250° SCO* 350' 400' 450° 600°
p-7575 242-1 663-2 1588 3384 6520
According to the same authority, its average coefficient
of expansion 4 per degree C. is as follows : —
0-100° C. 0-200° C. 0 .300' C.
i- -0001815 -0001841 -0001866
•r 1/5510 1/5432 1/5359
Its specific heat in the liquid state is "03332 ; that of
the frozen metal (between - 78° and - 40° C.) is -0319
(Regnaait). Its electric conductivity is ^ of that of pure
silver (MattMesen). Its conductive power for heat is
greater than that of water, and is proved (by Herwig) to
be perfectly constant from 40° to 160° C. Its vapour
density (air of the same temperature and pressure = 1) is
6-676 (Dumas), or 100-93 for hydrogen = 1. Hence its
molecular weight (H5 = 2) is 201-86. The atomic weight,
by chemical methods, was found = 200-0 (Erdmann and
Marchand) ; hence mercury-vapour molecijee consist of
single atoms. Mercury does not appreciably absorb any
chemically inert gas.
Mercury is in constant requisition in the laboratory. It
is used for the collecting and measuring of gases, in the
construction of thermometers, barometers, and manometers,
for the determination of the capacity of vessels, and many
other purposes. In medicine it serves for the preparation
of mercurial ointment and of " hydrargyrum cum creta "
(the chief component of " blue pills ") ; both are obtained
by diligently triturating the metal with certain proportions
•f grease and chalk respectively until it is " deadened," i.e.,
■dbdivided into invisibly small globules (see below).
Alloyt. — Mercury readily unites directly with all metals
(except iron and platinum) into what are called amalgams.
In some cases the union takes place with considerable
evolution of heat and large modification of the mean pro-
perties of the components. Thus, for instance, sodium
when rubbed np with mercury unites with it with deflagra-
tion and formation of an alloy which, if it contains more
than 2 per cent, of sodium, is hard and brittle, although
Bodium is as soft as wax and mercury a liquid. Liquid
ttmnlgama of gold and silver are employed for gilding and
silvering objects of copper, bron2e, or other base metaL
The amalgam is spread out on the surface of the object
by means of a brush, and the mercury then driven off
by the application of heat, when a polishable, firmly
adhering film of the noble metal remains. Copper
amalgam containing from 25 to 33 per cent, of the solid
meta^ when worked in a mortar at 100' C, becomes highly
plastic, but on standing in the cold for ten or tw-elve hours
becomes hard and crystalline. Hence it is used for the
stuffing of teeth. A certain amalgam of cadmium is
similarly employed.
Oxiilts. — There are two oxides of mercury, namely, an oxide,
HgjO, called mcrcurons, aad another, HgO, called mercnrfo oxide.
The latter can be produced directly by keeping the metal for a long
tune in air at a temperature somewhat below its boilin? point,
vften the oxide is gradually formed as a red powdery Eolid. This
wild has long been known as " ted precipitate." or as menurius
16—3
prcteipitalut per ae. Priestley made the important JiscoTery that
the " precipitate " whcu heated to dnll redness is reduced to metal,
with evolution of what has since been known os oxygon gas ; but it
was reserved for Lavoisier to con-ectly interpret this experiment
and thus to establish our present views on the constitution of
atmospheric air. The oxide is easily prcjared by htating any
nitrate of the metal as loug as nitrous fumes are' seen to go olf
(when it remains as a scaly mass, black when hot, red after cooling),
or else by precipitating the solntiou of a mercuric salt with excess
of caustic potash or soda, when it comes down as au omori>hous
yellow jirecinitatc, which is free of coinbiucd water. Wercurous
oxide, a black solid, can be obtained only indircctlv, by the decom-
position of mercurous salts with fixed caustic alkalies. Botli oxides
are insoluble in water, but dissolve in certain, and combine with
allj aqueous acids with formation of merciiry salts and elimination
of water. . Thus, for instance.
The nitrates. — Wlien metallic mercury is set aside with its own
weight of nitric acid of 1 -2 specific gravity, at ordinary tempera-
tures, the normal mercurous salt Hg„(X03).; is gradually produced,
and after a day or two is found to have separated out in colourless
crystals. These are soluble (somewhat sparinglv) in water acidu-
lated with nitric acid, but are decomposed by tho action of pun:
water, with formation of difficultly soluble basic salts. *\\ hen
this salt (or the metal itself) is treated with excess of nitric acid it
is oxidized into mercuric nitrate Hg(N03)j, a white crj-stalliue salt,
readily soluble in water without decomposition.
The Sidphfitis. — Cold aqueous sulphuric acid does not act upon
mercury, but the hot concentratea acid converts it first into
mercurous and then into mercuric sulnhate, with evolution of
sulphurous acid.
Hgj + 2H^0, - 2H.0 + SOj + HgjSOj ,
Hg^O, + 2HjS0, - 2H,0 + SO, + 2HgS0< .
Both salts form white crj-stalline magmas. The mercurous salt
is difficultly soluble iu water, and consequently producible by
precipitation of the nitrate with sulphuric acid. The mercuric salt,
when treated with .vater, is decomposed with formation of a yellow
insoluble basic salt, which has long been known as turpelhum mine-
rede. Its composition is SOj. 3HgO when produced by excess of
hot water. Mercuric sulphate is of importance chiefly as forming
the basis for the manufacture of the two chlorides.
Th£ Chlorides. — These are both extensively used medicinal agents.
The mercuric salt, HgCIj, known in medicine as corrosive stib-
limate, is prepared by mixing the sulphate intimately with common
salt, and subjecting the mixture to sublimation, a little biuoxide
of manranese being added to oxidize the mercurous salt, which is
generally present as an impurity. The process is conducted in a
glass flask buried in a hot sand-betlt. 'W'tien the decomposition in
accomplished, the sand is removed from the upper half of the flask
and the temperature raised so that the chloride HgCl, produced
sublimes np and condenses in the upper part as a "sublimate."
The salt, as thus produced, forms compact crystalline crusts, which,
when heated, melt into a limpid liquid before volatilizing. It is
soluble in water, 100 parts of which at 10°, 20°, 100° dissolve 6-57.
7-39, 54 parts of salt Corrosive sublimate dissolves in 3 parts of
alcohol and in 4 parts of ether. This salt, on account of its
solubility in water, is a deadly poison, llercurous chloride, HgjCl-,
better known as "calomel" (from koAos, fair, and /icAiu, black,
because it becomes dead-black when treated with ammonia, mer-
curic chloride yieldin" a white product), is prepared by mixing
corrosive sublimate with the proper proportion of metallic mercury
(HgCl, : Hg) or mercuric sulphate witli salt and mercury in the
proportions of HgSO^ : Hg : 2NaCl, and subjecting the mixture to
sublimation in glass Hasks. The salt Hg„Clj is thus obtained in
the form of white, opaque, crystalline crusts, which, when heated,
volatilize, without previously melting, into a mLxture of HgCl,
and Hg vapour, which, on cooling, recorabine into calomel. For
medicinal purposes the sublimate is reduced to an impalpable
powder, washed with water to remove any corrosive sublimate that
may be present, and dried. Being insoluble in water, it acts far
less violently on the organism than mercuric chloride does. Its
action, no doubt, is due to its very gradual conversion in the
stomach into mercury aud corrosive sublijnate. Finely divided
calomel can be produced, without trouble, by the precipitation of a
solution of mercurous nitrate with hydrochloric acid or common
salt ; but this preparation is liable to be contaminated with
mercurous nitfcte, and, even when pure, has been found to act far
mon; violently than ordinary calomel docs. Hence its use is not
tol.erated by the pharmacopoeias. According to ^Vohler a mercurous
chloride, more nearly equivaleut to the sublimed article, is produc-
ible by heating corrosive sublimate solution with sulphurous arid —
aHgClj + H^, -f H,0 - HjSO, + 2HC1 H- Hg,Cl, .
34
m E R C U R Y
The writct 'is unable to say whether "W'bhler's calomel has over
founU its way unywhero into medicinal practice.
The lodid'-.b. — The mercuii\. Rfllt HgL is produced iu two ways,
viz., first by mixing the two elementary components intimately
and suljjucting the mixture to sublimation, and secondly by pro-
cipitating corrosive sublimate solution with its exact equivalent of
iodide of potassium. In the fii-st case the salt is obtained in yellow
crystals, which, on the slightest touch with a solid bodj', assume
and then permanently ret.iin a rich scarlet colour. The precipita-
tiOQ process at once yields the scarlet salt. The salt is insoluble
in water, but soluble in alcohol and in iodide of potassium solution.
Tiie mercurous salt Hgjij is obtained by precipitating mercurous
nitrate with iodide of potassium as a dirty-greeu powder iusoluble
in water. Both iodides are used medicinally.
The Sulphides,— 'Mcvcnxom sulphide, HggS, does not seem to
exist. The mercuric salt, HgS, exists in two modifications, of
which one is amorphous and has a black colour, while the other is
crystalline and rod. The black one is obtained by precipitation of
solutions of mercuric salts with excess of sulphuretted hydrogen,
or by direct synthesis. The right proportions of mercury and
flowers of sulphur are rubbed together in a mortar until the whole
Is converted into a jet-black uniform powder. This preparation
(the xtkiops mincralis of the pharmaceutist), however, is apt to be
contaminated with uucombinod sulphur and mercury. Application
of a gentle heat causes exhaustive combination. The red sulphide,
HgS, occurs in nature as cinnabar, and can be produced artificially
from the black. The artificial preparation, known as vermilion, is
highly valued as the most brilliant, stable, and innocuous of all
mineral red jiigments. Vermilion can bo produced fi'ora the black
sulphide in two ways, viz., first by sublimation, and secondly by
treatment of it with fixed alkaline sulphide solution. According
to Bruuner, 100 parts of mercury are mixed intimately with 38 parts
of flowers of sulphur, and the aethiops is digested, with constant
agit-ation, in a solution of 25 parts of potash in 150 parts of water at
45° 0. (the water lost by evaporation being constantl}' replaced), until
the preparation has corae up to its maximum of fire and brilliancy,
which takes a goorl many hours. Purely sublimed vermilion has a
comparatively dull colour, and must be manipulated with alkaline
sulphide solution to give it the necessary fire. The action of the
alkaline sulphide consists probably in this, that it dissolves succes-
sive instalments of the amorphous preparation and redeposits them
in the crystalline form.
Mercuric Derivatives of Ammonia. — (1) Recently precipitated
oxide HgO is digested, cold, in cavbonic-acid-free ammonia, and
the mixture allowed to stand for a few days. The liquor is then
decanted off, and the precipitate washed with alcohol and then
with ether, and dried over sulphuric acid. The product is a
yellow solid base (" Millon's base ' ) of the composition
NaHg + 4HgO + H.O = NaHg^O . 2H,0 + 2H2O .
It is insoluble in alcohol and in ether, and requires 13,000 parts
of cold water for its solution. It readily unites with all acids,
forming salts, which, as a rule, are insoluble in water. Hence all
ordinary salt solutions, when shaken with the base, are decomposed
with elimination of the base of the salt. Thus, for instance, even
such salts as alkaline nitrates, chlorides, or sulphates are decom-
posed with formation of solutions of caustic alkali.
(2) A body N2Hgjl3 + 2H20, i.e.., of the composition of the iodide
corresponding to the oxide in (1), is produced as a brown precipitate
whftn ammonia or an ammonia salt is added to a solution of mercuric
iodide in iodide of potassium mixed with large excess of caustic
potash or soda (" Nessler's reagent"). In very dilute solutions of
ammonia Nessler's reagent produces only a brown or yellow color-
ation, which, however, is so intense that iniiro'oooo^^b of ammonia in
about 60 cubic centimetres of liquid becomes clearly visible.
(3) The chloride NHaHg.Cl of the " ammonium " NH„Hg is
produced as an insoluble white precipitate when ammonia is added
to a solution of corrosive sublimato. This substance is kntjwn in
medicine as infusible white precipitate, in contradistinction to (4)
(4") The fusible white precipitate was at one time supposed to be
identical with (3), and is obtained by boiling it with sal-ammoniac
solution. Its composition is NHoHgCl + NH^Cl^NaHe. Hg. CL.
Analysis. — Any ordinary solid mercury compound, when heaisd
in a Sliblimation tube with carbonate of soda, yields a sublimate of
metallic mercury, which, if necessary, needs only to be scraped
together wilh a wooden spill to unite into visible globules. From any
raercpry-salt solution the mptal is precipitated by digestion with a
piec^ot bright copper-foil. The precipitated mercury forms a coat-
ing on the copper, which becomes silvery on being rubbed with
blotting pai>er. When the quicksilvered copper is heated in a sub-
iini"*ion tuoe, il roassumes its'red colour with formation of a sub-
limate of mercury.
Solutions i;f mercurous salts with hydrochloric acid give a white
precipitate of calt^nn.'!, which, after filtration, is easily identified by
its becoming jot-blaok on troatmont with ammonia. From mercuric
solutions hydrochloric acid precipitalos nothing: but stannous
'dJoride. iu its twofold capacity as u chloride aud a reduciu;; agenl^
yields a precipitate of calomel. On addition of qu excess of reagent
the precipitate becomes grey through conversion into finely divided
quicKsilver. Sulphuretted hydrogen, when added very gradually
to an acid mercuric solution, gives at first an almost white precipi-
tate, which, on addition of more and more reagent, assumes suc-
cessively a yellow, orange, and at last jet-black colour. The black
precipitate is HgS, which is identified by its great heaviness,
and by its being insoluble iu boiling nitric and in boiling hydro-
chloric acid. A miiture of the two (aqua regia) dissolves it aa
chloride. (W. D.)
Therapeutics of Mercury.
The use of mercury as a therapeutic agent is of com-
paratively recent date. To the Greeks and Romans ita
value was unkno^\'n, and the Arabian physicians only used
it for skin affections. It was not till tile middle of the
16th century that the special properties of mercury were
fully appreciated, but since that time the metal has con-
tinued to hold a high though fluctuating value as a •
medicine. At first the metal in a finely divided state or
in vapour was used ; but very soon its various compounds
were found to be endowed with powers even greater than
those of the metal itself, and with the discovery of new
compounds the number of mercurial medicines has largely
increased.
The preparations now in use may be thus classified. (1)
Of the preparations containing metallic mercury the chief
members are blue pill (pilula hydrargyri), grey powder
(hydrargyrum cum creta), and blue ointment (unguentum
hydrargyri). The first- consists of mercury, liquorice root,
and coniection of roses, the second of mercury and chalk,
the third of mercury, suet, and lard. The power of the
tliree preparations seems to depend on the fine state of
subdivision of the mercury they contain ; mercui*y in its
ordinary liquid state seems devoid of medicinal properties.
It is thought by some that the fine subdivision of the
metal leads to the formation of a little oside, aud that the
efficacy of the preparations in part depends on this. (2)
Three oxides of mercury are employed in medicine, — the
red, from which \s> made red precipitate ointment (ungueu-
tum hydrargyri oxydi rubri), the yellow, an allotropic form
of the red, and the black oxide. The yellow and black
oxides suspended in lime water form respectively yellow
and black wash (lotio flava and lotio nigra). (3) The
chlorides of mercury form a very important group :
calomel (hydrargyri subcUloridum) is a white heavy
powder ; corrosive sublimate (hydrargyri perchloridum) is
a heavy crystalline substance, (4) Two iodides are used
medicinally ; they are known from their colour as the
green and red iodides. (5) Nitrate of mercury enttjrs into
the composition of a powerful caustic known as the acid
nitrate of mercury. It is also the active pjrinciple of citrine
ointment (unguentum hydi-argyri nitratis). (6) In this class
only ammoniated mercury and ita ointment commonly
known as white precipitate ointment, are contained. Of
the many compounds not included in the above classifica-
tion the oleate and albuminate are the most important.
Mercurial preparations are largely employed as external appli-
cations. Several of them are potent agents for the destruction of
the lower forms of animal life, and hence are employed to destroy
parasites having their habitat in skin, hair, and clothing. The
while and red precipitate ointments are specially effective" in the
destruction of pediculi, and blue ointment is occasionally used for
the same purpose. Corrosive sublimate is, however, the most
energetic of the mercurial parasiticides, and recent observations
seem to show that it is sujierior to almost all other substances as
a germ destroyer. It is sometimes used to get rid of ringworm-
It should be remembered that corrosive sublimate is a powerf"'
irritant to the skin, and also an active poison.
Acid nitrate of mercury is a caustic, aud by it warts and small
growths are soraetimea removed ; it is also ono of the caustics occa-
sional 1 /applied to prevent the spread of lupus.
In skin diseases mercurial preparations are larcely used, especially
in some forms of eczema. A few grains of the red oxido or of
ammoniated mercury in an ounce of zinc ointment 'are often found
of great service in this ailment ; citrino ointm-jnt is also uscfuL
M E R — M E R
35
Ctlomel ointment is not irritating, but ratlier tends to soothe. It
is therefore sometimes applied to irritable rashes ; in pruritus ani
it is of special value. Mercurial preparations are not -usually found
of benefit in scaly eruptions. In acne a neak solution of contteiTe
gnblimate is often most effective.
Preparations of mercury are often used to heal ulcers, especially
those of syphilitic origin. Black wash is one of the commonest
applications for this purpose. The red o.xide ointment is at times
employed to stimulate indolent ulcei^, and it is capable of remov-
ing exuberant granulations (proud flesh), which sometimes retard
the healing of wounds.
Mercury is largely used externally to promote the absorption of
inflammatory products, especially in the neighbourhood of joints.
The blue ointment is frequently employed for this purpose, more
rarely a plaster containing mercury or a mercurial liniment. For
effecting the absorption of goitre (Derbyshire neck) the ointment
of the red iodide is often relied on, especially in India, where it is
customary to expose the patient's neck to the sun after rubbing it
with the ointment. In enlargements of the liver and spleen the
application of mercurial ointment sometimes seems to promote I'e-
duction in size.
Taken internally in continued doses, mercury produces a peculiar
effect known as salivation. First a metallic taste is c.tperienced ;
this is followed by soreness of the gums, an undue flow of saliva,
and foetor of the breath. Further administration of the drug may
increase greatly the salivary flow, and also lead to swelling of <the
tongue, ulceration of the mouth, and even disease of the jaw-bone.
At the same time the blood becomes impoverished, and feverishness
with loss of flesh occurs. A single large dose — rarely too.a single
small dose — may produce some of the above symptoms. They may
also follow the inlialation of the metal or its compounds, or their
absorption through the skin. The long-continued inhalation of
the vapour of mercury acts likewise on the nervons system, caus-
ing a jieculiar kind of trembling. Mercurial tremor is sometimes
seen in looking-glass makers, often in those who work in quick-
silver mines.
Internally mercury is chiefly given for two purposes — (1) to
check inflammation and cause tho absorption of the products it
gives rise to, and (2) to antagonize the syphilitic virus and remove
the evils it causes. Some years ago the belief in the power of
mercury to control inflammation was almost universal, and it was
largely administered in almost all inflammatory affections, but of
late it has been much less used, both because it seems doubtful
whether it has really the power it was once supposed to have and
because- of ■ the possibility of evil results from its continued use-
In peritonitis and iritis it is still often employed, small doses of
calomel being given. Not unfreqnently too it is administered in
i<;ricarJitis and hepatitis, but in pneumonia, pleurisy, and most
other inflammatory affections its use is now discarded by many
jhysicians. As an antidote to the syphilitic poison it is still held
in high esteem, though opinions vary much as to the extent of its
power. There can be little doubt that, given in an early stage of
the disorder, it minimizes the secondary symptoms ; but it cannot
be relied on to prevent their occurrence. It aids in removing the
secondary symptoms, and tends to the avoidance of tertiary
manifestations, which nevertheless sometimes occur even when
mercury has been freely given. The custom of giving mercury
till profuse salivation is established has long been abandoned;
the aim now is so to give it as to prevent salivation occurring ; for
this purpose blue pill, calomel, and corrosive sublimate are given
in very small doses, but if the gums become tender the dose is
decreased or the administration stopped.
Mercurial treatment is sometimes carried out by rubbing the blue
ointment into the skin, sometimes by exposing the patient to- the
fumes of calomel ; syphilitic eruptions are often treated by such
fumigation. More rarely mercury is introduced by injecting the
albuminate or some other preparation under the skin or by means of
suppositories. In children grey powder is generally used when mer-
curial treatment is required. Children bear mercury well.
Blue pill, calomel, and grey powder are often used as purgatives,
and a power of promoting the 'secretion of bile is attributed to
them. Experimentally it has not been proved that they stimu-
late the liver functions, but there is good reason for believing that
they promote the expulsion of bile from the body. Grey powder is
especially valued as a mild and efficient aperient for clularen, and
is often given in the early stage of diarrhoea to expel the irritating
contents of the bowel.
The use of calomel in tropical dysentery, once very prevalent, has
within the last few years been abandoned. (D. J. L. )
MERGANSER, a word originating with Gesner {ffist.
Animalium, m. p. 129) in 1555, and for a long while used
in EngUah as the general name for a group of fish-eating
Dujiks possessing great diving powers, and forming the
genus ifergua of Linnaeus, now regarded by ornithologists
M a Subfamily, Utrginss, of the Family Anatida. The
Mergansers have a long, narrow bill, with a small but
evident hook at the tip, and the edges of both man-
dibles beset by numerous homy denticiSations, whence in
English the name of " Saw-biU " is frequently applied to
them. Otherwise their structure does not much depart
from the Anatine or FuUguline type. .All the species bear
a more or less developed crest or tuft on the head. Three
of them, Mergui merganser or castor, M. serraior, and M.
albellus, are found over the northern parts of the Old
World, and of these the first two also inhabit North
America, which has besides a fourth species, M. cxicuUatut,
said to have occasionally visited Britain. M. merganser,
commonly known as the Goosander, is the largest speciea/
being nearly as big as the. smaller Geese, and the adult
male in breeding-attire is a very beautiful bird, conspicuous
with his dark glossy-green head, rich salmon-coloured
breast, and the upper part of the body and wings black
and white. This fuU plumage is not assulned till the
secon^ year, and in the meantime, as well as in tl» poet-
nuptial dress, the male much resembles the female, having,
like her, a reddish-brown head, the upper parts greyish-
brown, and the lower dull- white. In this condition the bird
is often known as the " Dun Diver." This species breeds
abundantly in many parts of Scandinavia, Russia, Siberia,
and North -America, and of la-te years has been found to do
so in Scotland, usually making its nest in the stump of a
hollow tree or under a slab of rock. M. serrator, com-
monly called the Red-breasted Merganser, is a somewhat
smaller bird ; and, while the fully-dressed male wants the
delicate hue of the lower parts, he has a gorget of rufous
mottled -with black, below which is a patch of white
feathers, broadly edged -with black. The male at other
times and the female always much resemble the preceding.
It is more nunaerous than the Goosander, with a somewhat
more southern range, and is not so particular in selecting
a sheltered site for its nest. Both these species have the
bill and feet of a bright reddish-orange, while M. albellwi,
kno-wn as the Smew, has these parts of a lead colour, and
the breeding plumage of the adult male is white, with quaint
crescentic markings of black, and the flanks most beauti-
fidly vermiculated — the female and male in undress having
a general resemblance to the other two aheady described
— but the Smew is very much smaller in .'rize, and, so far
as is known, it invariably makes its nest in a hollow tree,
as ascertained first by Wolley {Ibis, 1859, pp. 69 rf seq.).
This last habit is shared by M. cucullatm, the Sooded
Merganser of North .America, in size intermediate between
M. alhellus and M. serrator, the male of which is easily
recognizable by his broad semicircular crest, bearing a fan-
shaped patch of white, and his elongated subscapulars of
white edged with black. The conformation of the trachea
in the male of M. merganser, M. serrator, and M. cucuUatus
is very like that of the Ducks of the genus Clangula, but
M. albellus has a less exaggerated development more
resembling that of the ordinary Fuligula} From the
southern hemisphere two species of Mergus have been
described, M. ocioseiacetts or hrasilianus, VieUlot {N. Diet.
dHist. Xaturelle, ed. 2, xiv. p. 222; Gal. des OUeanx,
* Hybrids between, as is presumed, M. albellus and Clangula
glaucum^ the common Golden-eye, have been described and figured
(Eirabeck, IHs, 1831, 300, tab. iii. ; Brehra, Nalurgtsch. alter Vsg.
DetUscklaruU, p. 930 ; Neumann, VGg. Deuischlands^ xii. p. 194,
frontispiece ; Kjserbolling, Jour. /Ur Omithologie, 1853, Extraheft,
p. 29, Naumannia, 1853, p. 327, OmitJwL Danica, tab. Iv., spppl.
tab. 29) under the names of -3/eryu5 ano^aniw, Clangula angustirostris,
and Anas (Clangula) mergoides, as though they were a distinct species ;
but the remarks of M. de Selys-Longchamps {BulL Ac. Sc. Bruxelles^
1845, pt. ii. p. 354, and 1856, pt. U. p. 21) leave little room for doubt
as to their origin, which, when the cryptogamic habit and common
range of their putative parents, the former unknown to the author last-
named, is considfxed, will seem to be still more likely.
36
M E R — M E R
torn, ii. p. 209, pL 283), inhabiting South America, of
which but few specimens have been obtained, having some
general resemblance to M. serrator, but much more darkly
coloured, and M. australis, Hombron and Jacqu6mont
(Ann. Sc. Nal. Zodogie, ser. 2, xvi. p. 320 ; Voy. au Pol
Slid, Oiaeaux, pL 31, fig. 2), as yet known only by the unique
example in the Paris Museum procured by the French
Antarctic expedition in the Auckland Islands. This last
species may perhaps be found to visit Nevr Zealand, and
should certainly be looked for there.
Often associated with the Mergansers is the genus
ilerganetta, the so-called Torrent-Ducks of South America,
of which three species are said to exist ; but they possess
spiny tails and have their wings armed with a spur.
WTiether they should be referred to the Merginas or the
Erismaiurinx — the Spiny-tailed Ducks proper — is a ques-
tion that further investigation must decide. (a. n.)
MERGUI, a district of British Burmah, between 9° 58'
and 13° 24' N. lat. It forms the southernmost district of the
Tenasserim division, and is bounded on the N. by Tavoy,
E. and S. by Siam, and W. by the Bay of Bengal, with
an area of 7810 square miles. Two principal ranges cross
Mergui from north to south, running almost parallel to
each other for a considerable distance, with the Tenasserim
river winding between them till it turns south and flows
through a narrow rocky gorge in the westernmost range
to the sea. Amongst these mountain ranges and their
subsidiary spurs are several fertile plains, densely clothed
with luxuriant vegetation. Indeed, the whole district, from
the water's edge to the loftiest mountain on the eastern
boundary, may be regarded as almost unbroken forest, only
73 square miles being under culthi'ation. The timber trees
found towards the interior, and on the higher elevations,
are of great size and beauty, the most valuable being teak,
ihen-gan (ffopea odorata), ka-gnyeng [Diplerocarpiis tuber-
tulatus), &c. The coast-lino of the district, studded vrith
»n archipelago of two hundred and seven islands, is much
broken, and for several miles inland is very UttlS raised
above sea-level, and is drained by numerous muddy tidal
creeks. Southv/ards of Mergui town it consists chiefly of
low mangrove swamps alternating with small fertile rico
plains. After passing the mangrove limits, the ground to
the east gradually rises till it becomes mountainous, even
to the banks of the rivers, and finally culminates in the
grand natural barrier dividing British Burmah from Assam.
The four principal rivers are the Tenasserim, Le-gnya,
Pakchan, and Palouk, the first three being navigable for a
considerable distance of their course. Coal is found in the
district on the banks of the Tenasserim and its tributaries.
Gold, copper, iron, and manganese are also found in various
parts of the district.
From the notices of early travellers it appears that Mergui, when
under Siamese rule, before it passed to the IJurmeso, was a rich and
densely peopled country. On its occupation by tlie British in
1824-25 it was found to be almost depopul.atcd — the result of
border warfare and of the cruelties exercised by the Burmese con-
querors. At that time the entire inhabitants only numbered 10,000 ;
in 1876 they had increased to 61,846 (26,767 males and 25,079
females). Classified according to religion, there were — Buddhists,
48,750 ; Mohammedans, 2533 ; Hindus, 353 ; Christians and others,
210. The district contains only one town (Mergui) with more than
5000 inhabitaNts. Only 73 square miles of the district area were
nnder cultivation in 1876, but this area is steadily though slowly
increasing. The principal manufactures are sugar-boiling and.tin-
amelting. Mergui carries on a flourishing trade with Rangoon,
Bassein, and the Straits Settlements. The chief cvports consist
of rice, rattans, torches, diicd fish, nreca-nuts, sesaunun seeds,
molasses, sea-slugs, edible birds' nests, and tin. The staple imports
are piece goods, tobacco, cotton, earthouwaro, tea, and sugar. The
imperial revenue in 1876 amounted to £18,208. The climate is
remarkably healthy, the heat duo to its tropical situation being
raoderateil by land and sea breezes. The rainfall in 1876 amounted
to 165^ inches. The prevalent diseases are simple and remittent
fevers^ bronchitis, rheumatism, and small-pox.
Mekoiji, chief town of the above district, is situated
on an island at the mouth of the Tenasserim river. The
population (10,731 in 1876-77) consists of many races —
Talaings, Burmese, Malays, Bengalis, Madrasis, Siamese,
and Chinese. Considerable trade is carried on with other
Burmese ports and the Straits Settlements. , The harbour
admits vessels drawing 18 feet of water.
MfiRIDA, a city of 7390 inhabitants (1877), in the
province of Badajoz, Spain, lies about 36 miles by rail
eastward from Badajoz, on the Madrid and Bj^Jajoz line,
on a small eminence on the right bank of the Guadiana.
It is connected by a branch line of rail with Llerena on
the south-east. The population is mostly agricultural.
The city owes its interest entirely to its Roman remains,
which are numerous and extensive. Of these one of the
most important is the bridge of 8 1 arches of granite, erected
by Trajan ; it is 2575 feet long, 26 feet broad, and 35 feet
above the bed of the river ; it was unfortunately seriously
injured diu'ing the siege of Badajoz in 1812. Of the
colossal wall that formerly surrounded the town all that
remains is a fine fragment, built of dressed stone, on the
spot formerly occupied by the castellum, and where the
provisor of the order of Santiago afterwards had his
residence (El Conventual). In the town are some relics of
temples of Diana, Mars, Fortuna, Jupiter, and others ; and
the Arco do Santiago, 44 feet high, also dates from Trajan's
time; it has unfortunately been stripped of its marble
casing. ' Of the aqueduct from the kguna of Albuera
thirty-seven enormous piers are still standing, with ten
arches in three tiers built of brick and granite. To the
east of the city is the circus, measuring some 1356 by 335
feet ; the eight rows of seats still remain. Further east-
ward is the almost perfect theatre, and near it are the
remains of the amphitheatre, or, as some prefer to call it,
naumachia (Bano de los Romanos).
Augusta Emcrita was built in 25 B.C. by the emeriti of the* fifth
and tenth legions who had served in the Cantabrian war under
Augustus. It rose to great splendour and impoi-tance as the capital
of Lusitania. During the Gothic period it became an episcopal see,
and several provincial councils known to history were held ther«.
It was taken by Mtisa in 711, and reconquered by Alphonso in 1228.
MERIDA, the capital of the Mexican state of Yucatan,
stands in a great plain in the north of the peninsula, on a
surface of limestone rock, about 25 miles from the port of
Progreso on the Gulf of Mexico, with which it is connected
by a railway opened in 1880. It is a well-built city, with
broad streets and squares ; and the flat-roofed stone houses,
after the style introduced by the Spaniards, give a Moorish
colour to the general view. Besides the cathedral, an im-
posing edifice of the 16th century, the bishop's palace, and
the Government house (all of which are situated in the prin-
cipal square! the most notable building is the Franciscan
monastery (1547-1 600),. which once harboured within its
high and turretetl walls no fewer than two thousand friars,
but has been allowed to fall into complete decay since
their expulsion in 1820. For a long time Merida has had
the reputation of being one of the principal seats of culture
in Blexico ; and it possesses, besides the ecclesiastical
seminary, schools of law, medicine, and pharmacy, a literary
institute, a public library, a theatre, and a considerable
number of periodical publications. Commercially it has
shared in the prosperity which Yucatan in recent years owes
to the development of the Sisal hemp trade ; and its manu-
factures embrace cotton goods, cigars, sugar, and rum. The
population, estimated about ,1840 as 25,000, was found
in 1871 to number 33,025. The Mayas still form numeri-
cally the strongest element. Previous to tho Spanish
conquest the site of Merida was occupied by the Maya
town of Tehoo, which contained so great a number of
artificial etone-mounds that the new-comers had abundant
material for all their buildings. The foundation of the
M E R.^M E R
37
ciW'dates froia* 1542, and it was made a bishopric in
J 561^ Compare Stephen's Tttcatan.
MERIDEN, a city of the United States, in New Haven
county, Connecticut, 18 miles from New Haven by rail
It is a busy manufacturing town ; the population has
increased from 3559 in 1850 to 7426, 10,495, and 1.8,340
in 1860, 1870, and 1880. The Britannia Company alone
employs upw'ards of 1000 hands, and sends out every year
nearly $3,000,000 worth of Britannia metal and electro-
plated goods ; and tin-ware, cutlery, brass-work, flint glass,
gur.8, and woollen goods are also manufactured in the town.
The State reform school had 307 inmates in 1880. A
fortified tavern erected by Belcher in 1660 on the road
between Boston and New Haven was the nucleus of
Meriden ; but the place was not incorporated as a town till
1866, and became a city in 1867.
JlfiRLMBE, Peospee (1803-1870), novelist, archseo-
logist, essayist, and in all these capacities one of the
greatest masters of French style during the century, was
bom at Paris on September 28, 1803, and died at Cannes
on the 23d of the same month sixty-seven years later,
having lived just long enough to know that ruin was
threatening France. Not many details have been published
in reference to his family, but his father seems to have
been a man of position and competence. M^rim^e had
English blood in his veins on the mother's side, and was
always considered, at least in France, to look and behave
mora like an Englishman than a Frenchman. He was
educated for the bar, but entered the public service instead.
A young man at the time of the romantic movement, he
felt its influence strongly, though his peculiar tempera-
ment prevented him from joining any of the c6teries of the
period. This temperament was indeed exhibited by the
very form and nature of the works in which he showed
the influence of romanticism. Nothing was more prominent
among the romantics than the fancy, as M^rimte himself
puts it, for " local colour," the more unfamiliar the better.
M^rim^e exhibited this in an unusual way. In 1825 he
published what purported to be the dramatic works of a
Spanish lady, Clara Gazul, with a preface stating circumstan-
tially how the supposed translator, one Joseph L'Estrange,
had met, the gifted poetess at Gibraltar. This was followed
by a still more audacious and still more successful
supercherie. In 1827 appeared a small book entitled La
Guda (the anagram of Gazul), and giving itself out
as translated from the lUyrian of a certain Hyacinthe
Maglanovich. This book, which has greater formal merit
than Clara Gazul, is said to have taken in Sir John Bow-
xing, a competent Slav scholar, the Russian poet Poushkin,
and some German authorities, although not only had it no
original, but. as M^rim^e declares, a few words of Illyrian
and a book or two of travels and topography were the
author's only materials. In the next year appeared a short
dramatic romance. La Jacquerie, in which all Mirimee's
characteristics are visible — his extraordinary faculty of
local and historical colour, his command of language, his
grim irony, and a certain predilection for tragic and terrible
subjects which was one of his numerous points of contact
with the men of the Renaissance. This in its turn was
followed by a still better piece, the Chronigue de Charles
IX., which stands towards the 16th century much as the
Jacquerie does towards the Middle Ages. All these works
were to a certain extent second-hand, being either directly
imitated or prompted by a course of reading on a particular
mbject. . But they exhibited aU the future literary qualities
of the author save the two chiefest, his wonderfully severe
and almost classical style, and his equally classical solidity
and statuesqueness of construction. For the latter there
was not much opportunity in their subjects, and the former
required a certain maturity amd self-discipline which
M^rim^e had not yet given to. himself. These were,
however, displayed fully in the famous Corsican story of
Colombo, published in the momentous year 1830. Tliis,
all things considered, is perhaps Merimie's best tale.
He had already obtained a considerable position in
the civil service, and after the revolution of July he was
chef de cabinet to two different ministers. He was then
appointed to the more congenial post of inspector of
historical monuments. M^rimfe was a born archaeologist,
combining linguistic faculty of a very unusual kind with
the accurate scholarship which does not always accompany
it, with remarkable historical appreciation, and with a sincere
love for the arts of design and construction, in the former
of which he had some practical skilL In his official
capacity he published numerous reports, some of which,
with other similar pieces, have been republished in his
works. He also devoted himself to history proper during
the latter years of the July monarchy, and published
numerous essays and' works of no great length, chiefly on
Spanish, Russian, and ancient Roman history. He did
not, however, negleet novel writing during this period, and
numerous short tales, almost without exception master-
pieces, appeared, chiefly in the Seirue de Paris. He travelled
a good deal, both for his own amusement and on official
errands ; and in one of his journeys to Spain, about th«
middle of Louis Philippe's reign, he made an acquaintanca
destined to influence his future life not a little — that of
Madame de Montijo, mother of the future empress Eugenie^
M^rim^e, though in manner and language the most
cynical of men, was a devoted friend, and shortly before the
accession of Napoleon IIL he had occasion to show this.
His friend Libri was accused of having stolen valuable
manuscripts and books from French libraries, and M^rim^
took his part so warmly that he was actually sentenced
to and underwent fine and imprisonment. He hai^ been:
elected of the Academy in 1844, and also of the Academy,
of Inscriptions, of which he was a prominent member.
Between 1840 and 1850 he wrote more tales, the chief
of which were Arsetie Guillot and Carmen.
The empire made a considerable difierence in M^rim^'ai
life. He was not a very ardent politician, but all hia
sympathies were against democracy, and he had therefore
no reason to object to .the Bonapartist nile, especially aa
his habitual cynicism and his irreligious prejudices
made legitimism distasteful to him. But the marriage
of Napoleon HI. ■with the daughter of Madame de
Montijo at once enlisted what was always the strongest of
M6rim^e'3 sjTnpathies — the sympathy of personal friend-
ship— on the emperor's side. He was made a senator, and
continued to exercise his archaeological functions ; but his
most important role was that of a constant and valued
private friend of both the "master and mistress of the;
house," as he calls the emperor and empress in his letters;
He was occasionally charged with a kind of irregular
diplomacy, and once, in the matter of the emperor's
Cmsar, he had to pay the penalty frequently exacted from
great men of letters by their political or social superiors
who are ambitious of literary reputation. But for the
most part he was strictly the " ami de la maison." ■ Ati
the Tuileries, at Compifegne, at Biarritz, he was a con^
stant though not always a very willing, guest, and his
influence over the empress was very considerable and Was
feaflessly exerted, though he used to call himself, in imitar
tion of Scan-on, " le boirSon de sa majesty." His occupax
tions during the last twenty years of his life were numerous
and important, though rather nondescript. He found,
however, time for not a few more tales, of which more will
be said presently, and for two correspondences,, which are
not the least cf his literary achievements, while they have
an extraordinaiT interest of matter. ._ One of these conaista
38
M E K — M E R
of the letters wliich have been published as Lettres a une
Inconnne, the other of the letters addressed to Sir Antonio
Panizzi, the late librarian of the British Museom. Various,
though idle and rather impertinent, conjectures have been
made as to the identity of the inconnue just mentioned.
It is sufficient to say that the acquaintamce extended over
many years, that it partook at one time of the character
of love, at another of that of simple friendship, and that
Mdrim^e is exhibited under the most surprisingly diverse
lights, most of them more or less amiable, and all interest-
ing. The correspondence with PanLzzi has somewhat less
personal interest. M^rim.iSe made the acquaintance origin-
ally by a suggestion that his correspondent should buy for
the Museum some MSS. which were in the possession of
Stendhal's sister, and for some years it was ckiefly confined
to correspondence. But M(5rimi$e often visited England,
where he had many fdends (among whom the late Mr
EUice of Glengarry was the chief), and certain similarities
of taste drew him closer to Panizzi personally, while during
part of the empire the two served as the channel for a
kind of unofficial diplomacy between the emperor and
certain English statesmen. These letters are full of shrewd
aperpis on the state of Europe at different times. Both
series abound in gossip, in amusing anecdotes, in sharp
literary criticism, while both contain evidences of a cynical
and Rabelaisian or Swiftian humour which was- very strong
in M&'imfe. This characteristic is said to be so prominent
in a correspondence with another friend, which now lies in
the library at Avignon, that there is but little chance of its
ever being printed. A fourth collection of letters, of much
Inferior extent and interest, has been printed by M. Blaze
de Bury under the title of Lettres a une autre Inconnue.
In the latter years of his life Mi!rim(5e suffered very much
from ill health. It was necessary for him to pass all his
winters at Cannes, where his constant companions were two
aged English ladies, friends of his mother. The terrible
year fouud him corhpletely broken in health, and anticipating
the worst for France. He lived long enough to see his fears
realized, and to express his grief in some last letters, and
he died on September 23, 1870.
Merim^e's character (which has been unwarrantably slandered
by those to whom political differences or his sarcastic istolerance
of '• posG " in literature made hiru obnoxious) was a peculiar and in
some respects an unfortunate one, but by no means unintelligible,
and perhaps iu a minor degree not uncommon Partly by tempera-
meut, partly it is said owing to some chihiish experience, when he
discovered that be had been duped and determined never to be so
again, not least owing to the example of Beyle, who was a friend
of his family, and of wliom he saw much, Merimee appears at a
comparatively early age to have imposed upon himself as a duty the
maintenance of an attitude of sceptical indifference and sarcastic
criticism. He certainly succeeded. Although, as has been said, a
man 'of singularly warm and affectionate feelings, he obtained the
credit of being a cold-hearted cynic ; and, although he was both
independent and disinterested, be was abused as a hanger-on and
toad-eater of the imperial court. Both imputations were wholly
undeserved, and indeed were prompted to a great extent by the
resentment felt by his literary equals on the otbor side at the cool
ridicule with which he met them. But he deserved in some of the
bad as well as many of the good senses of the term the phrase which
we have applied to him of a man of the Renaissance. He had the
warm partisanship and amiability towards friends and the scorpion-
like sting for his foes, he had the ardent delight in learning and
especially in matters of art and belles lettres; he had the scepticism,
the voluptuousness, the curious delight in the contemplation of tho
horrible, which marked tho men of letters of the humanist pcried.
Like them he was a man of the world, and a man who without any
baseness liked a king's palace better than a philosopher's hovel.
Like them he had an acute judgment in matters of business, and like
them a shigular consciousness of the nothingness of things. Even his
literary work has this Renaissance character. It i.s tolerably ex-
tensive, amounting to some seventeen or eighteen volumes, but its
bulk is not great for a life which was not short, and which was
occupied at least nominally in little else. About a third of it con-
sists of the letters already mentioned, which will always be to
those who delight in personal literature the most attractive part,
and which, ili"ii;;U iu a fragmentary fashion, are really important
.13 throwing side lights on history. Kather more than another third
consists of the ofhcial work which has been already alluded to —
reports, essays, short historical sketches, the chief of which latter is
a history of Pedro the Cruel, and another of the curious pretender
known in Russian story as the false Demetrius. Some of the
literary essays, such as those on Beyle, on Turguenief, &c., where
a personal element enters, are excellent. Against others and against
the larger liistorical sketches — admirable as they are — M. Taine's
criticism that they want life has some force. They are, however,
all marked by Merimee'sadniirablestylc, by his sound and accurate
scholarship, hia strong intellectual grasp of whatever he handled,
his cool unprejudiced views, his marvellous faculty of designing and
proportioning the treatment of his work. It is, however, in the
remaining third of his work, consisting entirely of tales either in
narrative or in dramatic form, and esjiecially in the former, that his
full power is perceived. He translated a certain number of things
(chieHy from the Russian) ; but his fame does not rest on these, on
his already-mentioned youthfill supercheries, or on his later semi-
dr.imatic works. There remain about a score of tales extending 131
point of composition over exactly forty years, and in length ironi
that of Colomba, the longest, which fills about one hundred and fifty
pages, to that of V EnUvement de la EcdoiUc, which fills just half
a dozen. They are unquestionably the best things of their kind
written during the century, the only noiivetles that can challeuge
comparison with them being the very best of Gautier, and one or
two of Balzac. The motives are sufficiently different. In Colombo.
and Mateo Falcone, the Corsicau point of honour is drawn on ; in
Carmen (written apparently after reading Borrow's Spanish books),
the gipsy character ; in La Venus d'lUc and Lokis (two of the
fiuest of all), certain grisly superstitious, in the former case that
kuown in a milder fcH'm as the ring.giveu to Venus, in the latter a
variety of the were-wolf fancy. Arsinc Gnillol is a singular satire
full of sarcastic pathos on popular niorahty and religion ; Ln
Chamhre JBleuc, an 18th-century conic, worthy of CrebiUon for
grace and wit, and superior to him in delicacy ; The Capture 0/ tJu-
itcdouH just mentioned is a perfect piece of desciiption ; L'Abb6
Anhain is again satirical ; La Double Meprise (the authorship of
which was objected to Blerimee when he was elected of the
Academy) is an exercise in analysis strongly impreg^nated with
the spirit of Stendhal, but better written than anything of that
writer's. These stories, with his lettei-s, assure lleriniee's ])lace in
literature at the very head of the French prose writers of the century.
He had undertaken an edition of Brantome for the Bibliothfeque
Elzevirienne, but it was never completed.
Blerimee's works have only been gradually published since his
death. The latest. The Letters to Panizzi, which have also ap-
peared in English, bears date 1881. There is as yet no uniforDi
or handsome edition, but almost everything is obtainable iu the
collections of Mfif. Charpentier and Calmann Levy. (G. SA.)
MERINO. See Sheep and Wool.
MERIONETH (Welsh Meiiionydd), a maritime county
of North Wales, is bounded N. by Carnarvon and Denbigh,
S.E. by Denbigh and Montgomery, and W. by Cardigan
Bay. It is triangular in shape, its greatest length north-
east to south-west being 45 miles, and its greatest breadth
north-west to south-east about 30 miles. The area is 385,291
acres, or about 600 square miles. Next to Carnarvon, Meri-
oneth is the most mountainous county in Wales. If the
scenery is less bold and striking than that of Carnarvon,
it excels it in richness, variety, and picturesque beauty.
Its lofty mountains are interpenetrated by dark deep dells
or smiling vales. The outlines of its rugged crags are
softened and adorned by rich foliage. The sea views are
frequently fine, and rivers, lakes, and waterfalls add a
romantic charm to the valleys. The highest summits in
the county are the picturesque Cader Idris (which divides
into three peaks, — one, Pen-y-Gadair, having an altitude of
2914 feet), Aran Fawddwy (2955), Arenig-fawr (2818),
Moel-wyn (2566), Rhobell-fawr (2360). The finest valleys
are those of Dyfi, Dysyni, TalylljTi, Mawddach, and Festi-
niog. The river Dyfrdwy or Dee rises 10 miles north-west
of Bala, and, after passing through Bala Lake, flows north-
east by Corwen to Denbighshire. The Dyfi rises in a small
lake near Aran Fawddwy, and expands into an estuary
of Cardigan Bay. The Mawddach or Maw, from the
north of Aran Fawddwy, has a course of 12 miles south-
west, during which it is joined by several other stream.s.
Tlie DwjTyd and other streams unite in forming the
estuary of Traeth Bach. The finest waterfalls are th«
M E R— M E R
39
Rhaiadi-y-GIyn near Corwen, Rhaiadr Du, and Pistyll
Cain, the latter 150 feet high. The lakes are very
numerous, but small, the largest being Bala Lake, or Pim-
blemere (in Welsh, Llyn Tegid, fair lake), i miles long by
1 broad, and Llyn Mwyngil (lake in a sweet nook) in the
Tale of Taly 11)11. Both are much frequented by anglers.
On account of frequent indentations the coast-line is about
100 miles long. Sandy beaches intervene between the
rocky shores Frequent shoals and sandbanks render
navigation very dangerous. There are only two harbours
of importance, Barmouth and Aberdovey.
A mountain tract of the county 15 miles from north to
south by 10 from east to west, stretching from the coast
inland, is of the Cambrian age, composed of grits, quartzose,
and slates, and comprising the Merionethshire anticlinal.
This tract is enclosed on the north, east, and south by the
Mencvian, Lingula, Tremadoc, and Arenig beds, which are
pierced by numerous dykes and intrusive masses, mostly
greenstone. Rhobell-fawi- is one of the greatest igneous
masses in the whole area of the Lingula beds. The Arenig
beds are interstratified with and overlaid by accumulations
of volcanic ashes, felspathic traps, or lava flows, which
form the rugged heights of Cader Idris, the Arans, the
Arenigs, Manod, and Moel-wyn ; and these are in turn
overlaid by the Llandeilo and Bala beds, the latter includ-
ing the Bala limestone. Extensive slate quarries are
worked near Festiniog, mostly underground, in strata of
the Llandeilo age, giving employment to about 4000 men.
Gold, lead, copper, and manganese have been obtained in
various places.
OHmau and Agriculture.— the climate varies much with the
elevation, in some places being bleak and cold, and iu others re-
Biarkably equable and genial. At Aberdovey. it is proverbially
Kiild, and the myrtle grows in the open air. All attempts to intro-
duce fruits have proved abortive in most parts of the county. The
•oil is generally thin and poor, with feitile tracts in the, valleys.
A great portion of the moss has been reclaimed within late years.
According to the agricultural returns for 1882, there were 154,406
acres, or considerably less than half the total area, under cultiva-
tion. Of this as much as 119,133 acres were permanent pasture,
and 13,755 under rotation grasses. Of the 17,312 acres under corn
CTops, 11,232 were under oats and '4807 under barley. Potatoes
occupied 2392 acres, and turnips only 1496 acres. The area under
woods extended to 15,049 acres.
The total number of horses in 1882 was 6088. A breed of
ponies is peculiar to this county and Montgomeryshire. The
rearing of horned cattle and dairy-tarming are largely carried on,
but the number of cattle (37,643) is considerably under the average
of Wales generally. On the other hand the nnmber of sheep in
1882 was 400,653, a larger number than in any other county of
Wales, and much beyond the general average in the principality.
They are a small hardy breed, which grow heavy fleeces. Goats
frequent the loftier crags.
According to the latest return the number of proprietors was 1695,
possessing 303,374 acres, with a gross annual value of £183,253. Of
the owners 1044, or 62 per cent. , possessed less than 1 acre, the
average extent of the propei-ties being 189 acres, and the average
value per acre a little over 12s. There were ten proprietors who
possessed over 5000 acres, viz., Sir "W. W. Wynn, 20,295 ; K. J. L.
Price, 17,718; T. P. Lloyd, 16,975; Mrs Kirkby, 13,410; Hon.
C. H. Wynn, 10,604 ; A. J. G. Corbet, 9347 ; Sir E. Buckley,
8738; W. E. Qakeley, 6018; W. 0. Gore, 5497; and R. M.
Kickards, 5701.
Manufactures. — Woollen goods are manufactured in various
places, especially at Dolgeily. They are principally coarse druggets,
kerseymeres, and flannels. The knitting of stockings was a great
industry at the close of last century, the value of the sales at Bala
being estimated at from £17,000 to £19,000 annually.
Railways. — The Cambrian Railway skirts the coast from Port-
madoc to Aberdovey. At Barmouth Junction a branch of the same
crosses to Dolgeily, where it is joined by a branch of the Great
Western Railway. Another branch of the Great Western unites
Bala and Festiniog, and the latter place has railway connexion both
with Llandudno Jonction and with Portmadoe.
Administration arid Population. — Merionethshire comprises five
hundreds and thirty-three civil parishes. It has one court of quarter
seasons, and the number of petty sessional divisions is six. Ecclesi-
astically it is partly in the diocese of Bangor, partly in that of St
Aaaph. The county returns one member to parliament. . There is
no municipal or parlinineutary borough. The towns returned in
1881 as urban sanitai-y districts are Bala (1663), Barmouth (1512),'
Dolgeily (2457), Festiuiog (11,272), and Towyu (3363), ' Since
1801 the population has nearly doubled. From 29,506 iu that year
it had increased in 1S51 to 38,963, iu 1871 to 46,598, and in 1881
to 54,793, of whom 27,576 wfie males and 27,217 females.
History and Anlijuilics. —OrigiuMy Merioneth belonged to the
territory of the Ordovices, and under the Uomans it was included
in Britannia Secunda. There are mauy Celtic, Roman, and luedi-
leval remains. Caer Drewj'n on the Dee, near Corwen, was a British
camp. There are numerous cromlechs in various parts of the county.
especially near the sea-coast. The Fia Occidcntatis of the Romans
passed through ilerioneth from south to north, and at Tomen-
y-Mur was joined by a branch of the South Watling Street, the
Castell Tomen-y-Mur being supposed to be identical with the
Roman station of Heriri Mens. -The immense ruin of Castel-y-
Bere was originally one of the largest castles iu Wales, but has not
been occupied since the time of Edward 1. During the Wars of the
Roses the castlo of Harlech, still a fine ruin, was held by the
Lancastrians, and was the last in Wales to surrender. Of ecclesi-
astical remains the most importantisCymmer Abbey, founded by the
Cistercians in 1198, a very fine ruin containing architecture of
various periods from Nonnan to Perpendicular. There are numer-
ous iuteiestiug old churches.
MERLIN. See Falcon.
MERMAIDS AND MERMEN, in the popular mythology
of England and Scotland, are a class of beings more or less
completely akin to man, who have their dwelling iu the sea,
but are capable of living on land and of entering into social
relations Avith men and women.' They are easily identified,
at least in some of their most important aspects, with the
Old German Meritninni or Meerfrau, the Icelandic Hafgufa,
Margygr, and Marmeimill (mod. MarbendLU), the Danish
Hafmand or Maremind, the Irish Merrow or Merruach,
the Marie-Morgan of Brittany and the Morforwyn of
Wales ; - and they have various points of resemblance to
the vodyauy or water-sprite and the rusalka or stream-fairy
of Russian mythology. The typical mermaid (who is
much more frequently described than the merman) has the
head and body of a woman, usually of exceeding loveliness,
but below the waist is fashioned like a fish with scales and
fins. Her hair is long and beautiful, and she is often
represented, like the Russian rusalka, as combing it with
one hand while in the other she holds a looking-glass. At
other times, like the rusalka, she is seen engaged in the
more prosaic occupation of washing or beating clothes ; but
this, as, for example, in Hugh Miller's terrible Loch Slin
legend, is a sign of some impending calamity. For a time
at least a mermaid may become to all appearance an ordi-
nary human being ; and from a very striking Irish legend
("The Overflowing of Lough Neagh and Liban the Mer-
maid," in Joyce's Old Celtic Romances) it is evidpt that a
human being may also for a time be transformed into a
mermaid.
The mermaid legends, both English and other, may be
grouped as follows. A. A mermaid or mermaidg either
voluntarily or under compulsion reveal things that are about
to happen. Thus the two mermaids (merewip) Hadebunj
and Sigelint, in the JSibelungenlied, disclose his future
course to the hero Hagen, who, having got possession of
their garments, which they had left on the shore, compel!
them to pay ransom in this way. According to Resenius,
a mermaid appeared to a peasant of Samsoe, foretold the
birth of a prince, and moralized on the evils of intem-
■' ^ The name mermaid is compounded of the A.-S. mere, a lake, and
magd, a maid ; but, though mere wt/occurs in Beowulf, mere-maid docs
not appear till the Middle English period (Chaucer, Romaunt of the
Roee, &c ). In Cornwall the tjshermen say merry-maids and merry-
BK». The connexion with the sea rather than with inland waters
appears to he of later origin. " The Mermaid of Martin Meer "
(Roby's Traditions of Lancashire, voL ii.) is an ciample of the older
force of the word; and such "meer-women" are known to the
country-folk in various parts of England {e.g., at Newport in Shrop-
shire, where the town is some day to be drowned by the woman's
agency). ' ''>^iVK;$tff'^^f' >
= See Bliys, " Welsh Fairy Tales," in T Cymmrodor. 1881, 1882.
40
M E R — M E R
perance, Ac. (Kon'j Fredmichs den. nndem KriinU-e,
Coijcnliagen, 1680, p. 302). B. ••( Mermaid imparts
supenuJtitrttl powers tn n human bmiy. Thus in the
beautiful story -of " The Old JIan of Cury " (in Hunt's
Popular Jiomances of the West of England, 1871) the old
man, instead of silver and gold, obtains the power of doing
good to hi.^ neighbours "by breaking the spells of witchcraft,
chasing away diseases, and discovering thieves. John
Reid, the Cromarty shipmaster, was more selfish, — his
"wishes three" being that neither he nor any of his
friends should perish by the sea, that he should be unin-
terruptedly successful in everything he undertook, and that
the lady who scorned his love should scorn it no more.
C. A mermaid has some one under her protection, and for
wrong done to her ward exacts a terrible penalty. One of
the best and most detailed examples of this class is the
story of the " Mermaid's Vengeance " in Mr Hunt's book
already quoted. D. A mermaid falls in love with a hitman
being, lives ivith him as Ms lauful wife for a time, and then,
some compact being unwittingly or intentionally broken by him,
departs to her true home in the sea. Here, if its mermaid
form be accepted, the typical legend is undoubtedly that
of Melusina, which, being made the subject of a fuU-fledged
romance by Jean d' Arras, became one of the most popular
folk-books of Europe, appearing in Spanish, German,
Dutch, and Bohemian versions. Melusina, whose name
may be a far-off echo of the Mylitta (Venus) of the
Phcenicians, was married to Raymond of Lusignan, and
was long afterwards proudly recognized as one of their
ancestors by the Luxembourg, Rohan, and Sassenaye
families, and even by the emperor Henry \J\. Her story
will be found in Baring Gould's Myths of the Middle Ages.
E. A mermaid falls in love %Dith a man, and entices him to
go and live with her below the sea ; or a merman wins the
afection or captures the person of an earthhorn Tnaiden.
This form of legend is very common, and has naturally
been a favourite with poets. MacphaU of Colonsay
successfully rejects the allurements of the mermaid of
Corrievrekin, and comes back after long years of trial to
the maid of Colonsay.' The Danish ballads are especially
full of the theme ; as " Agnete and the Merman," an ante-
cedent of Matthew Arnold's " Forsaken Merman" ; the
" Deceitful Merman, or Marstig's Daughter " ; and the
finely detailed story of Rosmer Hafmand (No. 49 in
Grimm).
In relation to man the mermaid is usually of evil issue
if not of evil intent. She has generally to be bribed or
compelled to utter her prophecy or bestow her gifts, and
whether as wife or paramour she brings disaster in her
train; In itself her sea-life is often represented as one of
endless delights, but at other times a mournful mystery
and sadness broods over it. The fish-tail, which in popular
fancy forms the characteristic feature of the mermaid, ia
really of secondary importance ; for the true Teutonic
mermaid — probably a remnant of the great cult of the
Vanir — had no fish-kail ; ^ and this symbolic appendage
occurs in such remote mythological regions as to give no
clue to historical connexion. The Tritons, and, in the
later representations, the Sirens of classical antiquity, the
Phcenician Dagon, and the Chaldajan Cannes are all well-
known examples ; the Ottawas and other American Indians
have their man-fish and woman-fi.sh (Jones, Traditions of
the North American Indians, 1830); and the Chinese tell
stories not unlike our own about the sea-women of their
Bouthorn seas (Dennis, Folk-lore of China, 1875)
Quasi-hiatorical instances of the appearance or capture of
_}' See'Leyilcn's "Tlie Mermaid," in Sir Walter Scott'a Border
Uinstnlsy. ■#**','
» Karl Blind, " New Finds io ShctUsJlc and 'Welsh Folk-Lore," in
Oenttefnan'g Magazine, 18S11.
mermaids are common enougb,^ and serve, with the frequent
use of the figure on signboards and coats of arms, to show
how thoroughly the myth had taken hold of the popuUir
imagination.' A mermaid captured at Bangor, on the
.shore of Belfast Lough, in the 6th century, was not only
baptized, but admitted into some of the old calendars as a
saint under the name of Murgen (Notes and Queries,
Oct. 21, 1882); and Stowe (Annates, under date 1187)
relates how a man-fish was kept for six months and mora
in the castle of Orforde in Suffolk. As showing how
legendary material may gather round a simple fact,
the oft-told story of the sea-woman of Edam is particu-
larly interesting. The oldest authority, Joh. Gerbrandua
a Leydis, a Carmelite monk (ob. 1504), tells (AniialeSj
(tc, Frankfort, 1620) how^ in 1403 a wild woman
came through a breach in the dike into Purmerlake, and,
being found by some Edam milkmaids, was ultimately
taken to Haarlem and lived there many years. Nobody
could understand her, but she learned to spin, and was
wont to adore the cross. Ocka Scharlensis (Chronijk vam
Friesland, Leeuw., 1597) reasons that she was not a fiah
because she could spin, and she was not a woman because
she could live in the sea ; and thus in due course she
got fairly established as a genuine mermaid, Vosmaer,
who has carefully investigated the matter, enumerates forty
WTiters who have repeated the story, and shows that the
older ones speak only of a woman (see " Beschr. van de
zoogen. Meermin der stad Haarlem," in Verh. van de. Holl.
Maatsch. van K. en Wet., part 23, No. 1786). As for the
stuffed mermaids which have figured from the days of Bar-
tholomew Fair downwards, it is enough to mention that
exhibited in the Turf Coffee-house, London, in 1822,
and carefully drawn by Cniikshank (comi»re Chambers,
Book of Days).
The best account of the Diermaid-myth iB in Baring Gfould'«
Mytlis of llu Middle Ages. See also, besides works already men-
tioned, Pontopjtidan, who in his logically credulous way collects
much matter to prove the existence of mermaids ; Maillet, Tdli-
amed, Hague, 1765 ; Grimm, Deutsche ilythologie, L 404, and
Altddn. Heldenlieder, 1811 ; Waldron's Description and Train'a
Hist, and Stat. Ace. of the hie of Man ; Folklore Society's Record,
vol. IL ; Napier, Hist, and Trad. Tales connected with the Sontk cf
Scotland; Si5billot, Traditions de la Haute Bretagne, 1882, an4
Conies des Marins, 1882. (H. A. W.)
MEROE, in classical geography (Strabo, xrii. 2, 2 ; Pliny,
ii. 73, V. 10 ; Ptol., p. 201), was the metropolis of ./Ethiopia,
situated on an island of the same name between the Nile
and the Astaboras (Atbara). The " island " is only an
inacciu^te name for the fertile plain between the two
rivers. This Meroe, first mentioned by Herodotus (iL 29
sq.), succeeded an older Ethiopian kingdom of Napata lower
down the Nile, originally subject to -and civilized from
Egypt, but which afterwards became independent and evea
sent forth an Ethiopian dynasty to reign in Egypt, to whick
the So and Tirhaka of the Bible belonged (see Ethiopia).
The name of Meroe in the form Merawi is now given to
Napata. The later Meroe retained its independence when
Egypt fell under foreign sovereigns. Diodorus (iii. 6)
describes it as entirely controlled by the priesthood till a
native prince Ergamenes destroyed the sacerdotal caste in
the time of Ptolemy II. Queen Candace (Acts viii. 27)
was probably sovereign of Meroe ; see Lepsius's Letters,
Eng. tr., pp. 196, 206; and comp. Strabo, xvii. 1, 54 for
^ Compare the strange account of the qnasi-human creatures found
in the Nile given by Theophylactus, Bistorim, viii. 16, pp. 299-302
of Bekker's ed. •> *«-»* ■ .m.-:.- '• ■
* See the paper in Jour. Brit. Arch. Ass., xxxviii., 1882, by H. 8.
Cunuiis;, wbe pointji out that mermaids or mermen OTcur in the arras
of Earls Caleiton, Howth, and Sandwich, Viscounts Boyne and Hood,
Lord Lyttleton, and Scott of Abbolsford, as well as in those of th«
Ellis, Byron, Pheni, SkeBington, and other families. The English
heralds represent the creatures with a single tail, 'the French and
German heralds frequently with a dauble one.
M E R — M E R
41
t, Queen Caudaco in Augustus's time when the Romans
under Petronius advanced to Napata. Meroe -nas visited
by Greek merchants ; and the astronomical expedition of
Eratosthenes determined its latitude with great accuracy.
An exploring party in the reign of Nero found that the
coimtry below Meroe, formerly the site of many towns,
had become almost wholly waste (Pliny, vi. 29). From
the 6th to the 14th century of our era the Christian
(Jacobite) realm of Dongola occupied the place of the older
kingdom. The ruins of Meroe and Napata were fully
explored by Lepsius- in 1844. and the monuments are
pictured in his Dmk-miilfr.
MERSEBURG, the chief town of a district of the same
name in the Prussian province of Sa.\ony, is situated on
the river Saale, 10 miles to the south of Halle and 17 to
the west of Leipsic. It consists of a quaint and irregularly
built old town, with two extensive suburb,s, and contains
six churches and several schools and charitable institxitions.
The cathedral is an interesting old pile, with a Romanesque
choir of tiie 11th, a transept of the 13th, and a Late GotJiic
nave of the 16th century. Among its numerous monuments
is that of Rudolph of Swabia, who fell in 1080 in an
encounter with his rival Henry IV. It contains two
paintings by Lucas Cranach. Contiguous to the cathedral
IS the Gothic chateau, formerly the residence of the Saxon
princes and the bishops of Merseburg. The town-house, the
post-office, and the " standehaus " for the meetings of the
provincial estates are also noteworthy buildings. The
industries of Merseburg consist of the manufacture of card-
board and coloured paper, dyeing, glue-boiling, machine-
making, calico-printing, tanning, and brewing. Its popu-
lation in 1880 ^vas 15,205,
Merseburg (i.e., *' march-town '*) is one of the olilest towns in
Germany. From the 9th' century down to 1007 it was tlie eapitnl
of acountship of its own name, and from 968 to 1543 it was the seat
ofabisliop. InthelOth, llth, and 12th centuricsitwasa favourite
residence of the German emperors, and at this time its fairs enjoyed
the importance afterwards inherited by those of Leipsic. Tlie to^vn
was repeatedly visited by destructive conflagrations in the 14th to
17th centuries, and also sutfered severely during the Tliirty Years'
War. From 1656 to 1738 it was the residence of the dukes of Saxe-
Merseburg. The great victory gained by the emperor Henry I.
over the Huns in 933 is believed to have been fought on the Kousch-
berg near Merseburg.
MERTHYR TYDFIL, or Mekthys -Tydvil, a parlia-
mentary borough and market-town of Glamorganshire,
South Wales, is situated in a bleak and hilly region on the
river Ta£E, and on several railway lines, 25 miles north-
north-west of CardifE and 30 east-north-east of Swansea.
The town, which consists principally of the houses of work-
men, is for the most part meanly and irregularly bviilt, and
at one time, on account of its defective sanitary arrange-
ments, was frequently subject to epidemics of great severity.
Within recent years great i.Tiprovements have taken place,
and the town now possesses both a plentiful supply of
pure water and an excellent system of sewage. There are
also some good streets with handsome shops, while in the
suburbs there are a number of private residences and villas
inhabited by the wealthier classes. Apart from its extensive
iron and steel works, the town possesses no feature of
interest. It is situated in the centre of the South Wales
coal basin, and the rich coal-mines in the vicinity supply
great facilities for the iron industries. At Merthyr Tydfil,
which is said to have received its name from the martyr-
dom of a British saint TydfU, there were smelting-works
at a very early period, but none of any importance until
1755. From about forty years ago until 1875 the manufac-
ture of bar iron developed with great rapidity, but since
then the production of steel has largely taken its place.
Tha borough rettums two members to parliament. The
population of the urban sanitary district in 1871 was
61,949, and in 1881 it was 48,857; the population of the
paruamentary borough, which includes the pariah *f Aher-
dare and parts of the parishes of Llanwonno and Merthjr
Tydfil and of Vainor (Brecon), and has an area of 29,954
acres, was in the same years 97,020 and 91,347.
MERV, Meru, or MAOtrii," a district of Central Asia,
situated on the border-land of Iran and Turan.
The oasis of MeiT lies in the midst of a desert, in about
37° 30' N. lat. and 62' E. long. It is about 250 miles
from Herat, 170 from Charjui on the Oxus, 360 from
Khiva, and 175 from Gawars, the nearest point in the
newly acquired (1881) Russian territoi-y of Akhal.
The great chain of mountains which, under the name of
Paropamisus and Hindu-Kiish, extends across the Asiatic
continent from the Caspian to China, and forms the line
of ethnic demarcation between the Turanian and Indo-
Germanic races, is interrupted at a single point ; that point
is on the same longitude with Jlerv. Through or near the
Neighbourhood of Merv.
troupe or gap which nature has created flow northward m.
parallel courses the rivers Heri-rud (Tejend) and Murghab,
until they lose themselves in the desert of Kara-kum — that
large expanse of waste, known also as Turcomania, which
spreads at the northern foot of the mountains, and stretche*
from the lower Oxus to the Caspian.
Whether as a satrapy of Darius and subsequently as
a province of Alexander, whether as the home of the
Parthian race, whether as a bulwark against the destructiT*
waves of Mongol invasion, or later as the glacis of Persian
Khorasan, the valleys of those rivers — the district of Merri
^ Merv is the modem Persian name. The river Margus, now tire
Murghab, ou which was built the ancient city, is derived from Margu^
the name of the province as recorded in the Behistan inscriptions of
Darius. Spiegel connects the name ilargv with old Bactrian nierepA«,
bird, in allasion to the numeroua swarms of birds that gather there.
So, too, the river name Murghab means bird-water. The district ap-
pears to hare been known in the 5th ceutury as Marv-i-rud, so that
the river was then the Marv. The name Merim for the district
occura in the Armenian geography ascribed to Moses of Khorene,
written probably in the 7th century (ed. Patkanoff ). Maonr is the
Uzbek Dame, and of comparatively recent date.
JV1. _ 6
42
]\I E R V
— have evei' been imiiortant outposts on the borders of
Iran. ^ Jn bye-gone epochs their banks have, under powerful
rulers, been .studded with populous and flourishing cities,
which lx)rc-the name of " Sovereign of the Universe " (Atero
Skiih-i-Jelian), and vied for fame with " Balkh, the Mother
of cities"; of late times, with weakness or absence of govern-
ment, those same banks have become choked with fallen
battlements and ruins, the home of the snake and the jackal.
Merv has soared to prosperity or fallen to decay accord-
ing to her political status at the moment, and history,
which repeats itself, may yet have to sing her praises" in
the future as it has done in the past. All that human
life in the desert requires is there, — water in abundance,
and a soil unsurpassed for fertility. Good government is
alone wanting to turn those natural gifts to full account.
The present inhabitants of the district are Turcomans
of the Tekke tribe, who, like the other tribes inhabiting
Turcomania, enjoyed until the approach of the Russians
virtual independence, and acknowledged allegiance to no
one, — a pastoral people who eked out a miserable existence
by the trade of passing caravans, and in bad times pillaged
the neighbouring and equally barbarous states, to whose
reprisals they were in turn subjected.
From the year 1869, the date of the establishment of
the Russian military settlement at Krasnovodsk on the east
shere of the Caspian, the wave of Russian conquest has
gradually swejit eastwards along the northern frontier
of Persia until it has for the moment stopped at the outer-
most border of the Akhal Turcoman country, which was
incorporated in 18S1 by Russia as the result of the defeat
of that tribe at Geok Tepe Among the districts still
farther east, to which the Russians give the name of
Eastern Turcomania, is that of the Merv Tekke Turcomans,
kinsmen of the Akhal Tekkes, the most recent of Russia's
subjects. • The district of the Merv Tekkes may be taken
to be tliat included between the lower llurghab below
Yulutan, where the river enters the plain, and the Persian
frontier from Sarakhs to Gawars.
A reference to the map will show the strategical import-
ance of this district, situated at the point of meeting of
two lines, of which one is the strategic line of Russian
advance on Herat from Krasnovodsk to Sarakhs, and the
other the strategic line of advance on the same place from
Tashkend through Bokliara. The capital of the district
is, moreover, the crossing-point of the Herat-Khiva and
Meshed-Bokhara trade routes.
Consequently 'this district, a solitary oasis in a vast
desert, guarantees to its possessor the command of an
important avenue between north and south, and, in the
event of its falling into Russian hands, will give that power
in axldition a valuable link in the chain of connexion
between her recent acquisitions on the Persian frontier
and those in Turkestan, the forging of which has been
persistently atlvocated by Russian writers for years past.
One of these. Colonel VeniukolF, frankly admits that it is
the pohtical results — " the consolidation of friendly relations
with the Turcomans " — and not commercial interests
merely, that are primarily looked to, and openly states
that the forward movement in Central Asia "cannot end
otherwise than by the annexation to Russia of the whole
of Turan."
Whether by design or by the force of circumstancci, the
recommendations of those writers have been translated into
facts, and Russia with her advanced post at Askabad is
now within 400 miles of Herat, which Sir Henry Rawlinson
designates as the key of India. The occupation of the
Merv Tekke country would bring Russia to within 2.50
miles of Herat. From Askabad she is in connexion with
the Caspian by a good lino of communication, part of which
from the sea to Ki7.il Aivat) is by rail ; and hence facilities
are offered for bringing up not only the resources of the
Caucasus but of the whole of European Russia, ^\^l^le
Russian troops are within 400 mUes of Herat, the British
troops at Quctta are more than 500 miles from Herat.'
These remarks serve to exjilain the very natural
suspicion with which Great Britain has regarded the
occupation one after another of important strategical
points along that route by which alone Russia can strike
at India, — the same line by which Naijoleon meditated a
Russo-French invasion in the early part of this century.
In the matter of Merv and the neighbouring Turcotnan districts
diiilomaey-h.as not been idle. As early as 1869, when an inter-
change of opinions was taking place between the Russian and
British Governments with respect to the demarcation of a neutral
zone between the two empires. Great Britain objected to the
Russian proposal that this zone should be Afgfianista-n, "because
of tlie near approach to India that would be thereby afforded to
Russian troops from the direction of the Kara-kum, the home of the
Turcomans, of which Merv is the central point." In the following
year a Russian diplomatist remarked to the British ambassador at
St Petersburg, when discussing the Afghan frontier, that great care
would be required in tracing a line from Khoja Saleh on the Oxus
to the south, as Mer\' and tlie country of the Turcomans were be-
coming "commercially important." About the same time Russia
intimated that, if the amir of Afghanistan claimed to exercise
sovereignty over the Tekkes, his pretensionscould not be recognized.
After the Russian campaign aoainst Khiva in 1873', and the sub-
sequent operations agahist the Turcomans, the English foreign
secretary early in 1874 called attention *'to the fears expressed by
the amir of Afghanistan as to the complications in which he might
become involved with Russia were the result of a Rilfesian expe-
dition against Merv to be to drive the Turcomans to take refuge in
tlie province of Badghces in Herat." In reply to this communi-
cation Prince Gortscliakoff repeated the assurance that the imperial
Government " had no intention of sending any expedition against
the Turcomans, or of occupying Merv." In 1375 the operations of
General Lomakin on the northern frontier of Persia led to represen-
tations being made by the British ambassador at the court of St
Petersburg. To these Russia replied that the czar had no inten-
tion of extending his frontiers on the side of Bokhara or on the
side of Krasnovodsk. Notwithstanding the oft-repeated assurances
to the contrary., large annexations have been since made in Turco-
mania by the Russians, and these proceedings, clearl}' indicating
the persistent prosecution of a concerted plan, have naturally tended
to disturb the harmonious relations which should subsist between
the two great civilizing powers of tlie East.
Settlements and Inhabited Centres. — Of towns or even
viUages, fixed centres of habitation, there are none, ac-
cording to Mr O'Donovan, the latest European traveller
to Merv. The [iresent political and military capital of
Merv is Koushid Khan Kala, a fort which serves rather as
a place of refuge against sudden attacks than as a habita-
tion. It is situated on the east bank of the most westerly
branch of the Murghab, about 2D mdes below the dam at
Porsa Kala. In form it Ls oblongj measuring 1^ miles long
by f mile broad, is constructed entirely of earth, revetted
on the exterior slope with smi-dried brick ; the ramparts
are 40 feet high, and are 60 feet at the base. The fort is
built in a loop of the river, which protects it on two sides ;
between it and the river is an " obah," or nomad village of
huts and tents, some thousand in number, disposed in rows,
but there is no town or settlement.
Twenty-five miles east of Koushid Ivlian Kala lie the
ruins of the Greek city of Antiochia Margiana, showing
traces of a high civilization. According to Strabo (xi. 2)
the Merv oasis at this period was surrounded with a wall
measuring 1500 stadia (185 miles). Mr O'Donovan found
the trace of the fort of Iskander to have been quadrangular,
with a length of side of 900 yards. This was probably the
fort built by Alexander, about 328 B.C., on his return from
^ ConcurrLMitly with the consolidation of her position in Turcomania,
Russia has of late been showing less military activity on the side of
her Turkestan district. It is probable that her recent explorations at
the sources of the Oxus have demonstrated the impracticability of
directing any offensive movement against India from that side.
Hence the line of strategical advance has been shifted from Tashkend
to TiUis.
M E R V
43
Sogdiana after the capture of Bessus, ^Tlie city was
destroyed in 666 A.D. by the Arabs, who built a new one,
afterwards known as Sultan Sanjar, about 1000 yards
away, and occupying an area, according to Mr O'Donovan,
of about 600 yards square. The towers are still extant,
and inside can be seen the ruins of a most elaborate tomb,
in which the supposed bones of Sultan Sanjar are enshrined.
It has always been a place of pilgrimage for the faithful.
Not far to the south-west lies the site of the last city of
Merv, that which existed up to a hundred years ago,
when it was laid waste by the Bokharians. It bears the
name of its gallant defender Bairam Ali.
These three ruins are all that remain of that which
flourished of yore as "sovereign of the universe."
At the time of the visit of Burnes, Abbott, Shakespear,
and Taylour Thomson, about the fourth decade of the
century, Merv was under the jurisdiction of Khiva, and
the administrative centre was at Porsa Kala, where the
dam is situated. This place is now also a waste of mud
ruins, uninhabited.
Rivers. — The Heri-rud (or Tejeud, as the river is
named below Sarakhs) runs a course of some 280 miles
within Afghan borders. On reaching the Persian fron-
tier it turns north and forces a channel through the
mountain chain near Sarakhs. Beyond Sarakhs the river
is Turcoman on both banks, runs close to the Khelat
mountains, and in the latitude of Askabad loses itself in
the marshes formed by the spring floods. It is probably
the Ochus of ancient geography, which watered Nissa, once
the capital of Parthia, and joined the Oxus just before
the latter river disembogued into the Caspian (Rennell's
Herodotus). The Tejend is fordable at all points below
Sarakhs except in the early spring after the melting of the
snows. On the road from Meneh to Merv the river is
sluggish, 50 yards wide and 4 feet deep in February. The
river-bed is sunk 12 to 15 feet below the level of the
surrounding country, and has immense quantities of drift
wood on its banks ; trees and luxuriant herbage clothe the
immediate borders. At midsummer the river runs nearly
dry, and does not reach Sarakhs. The Kashaf-rud, which
flows near Meshed, is one of its chief affluents.
The Murghab takes its rise in the northern slopes of the
Paropamisus, and runs parallel to the Heri-rud at a distance
of 70 miles from it. On this river lies the plain or oasis
of Merv, irrigated by means of an elaborate system of dams
and canals cut from the main river. Beyond the hmits
of the oasis the Murghab " hides its streams in the sand,"
like the Tejend. The river at Porsa Kala (near the
principal dam) is 80 yards wide, at Koushid Khan Kala 30
to 40 yards wide. In summer it is much swollen by the
melting of the snows, and its stream is then barely fordable.
The water is yellow in colour from suspended matter.
Formerly a great deal of the coimtry, now a waste,
between the two rivers was also cultivated by the agency
of water derived from canals cut from the Tejend. These
canals extended to Kucha Kum in the desert, rendering
the journey between the two rivers much easier than in the
present day. From the Murghab was also cut, among
others, the Kara-i-ab canal, which ran for a distance of 40
miles towards the Tejend. Recent explorers affirm that there
is no reason why these canals should not be again filled
from those rivers, when the intervening country, " an argO-
laceous expanse" (O'Donovan), would become culturable.
Communication. — Merv is surrounded on all sides by desert. On
Iho north, we.<tt, and east this desert is sandy and arid ; water is
ezceedinffly scarce, the wells being sometimes 60 or 70 miles apart,
and easily choked. To the south of Merv, between the nvers
Murghab and Tejend, there are traces of past cultivation, of irrisating
canals, and of considerable settlements. Between the Tejena and
Aakabad the road lies through a populous well -cultivated country
(Persian territorj-) by way of Kahka and LutfabocL
There are no roads in Merv,— nothing but mere tracks. Many
wide and deep inigating canals have to be crossed ; bridges ai-e few,
and bad. The inhabitants cross bv inflated skins.
The following tracks lead to thePcrsian frontier from Meiv : — (1)
via Mahmur or Chuiigul to Lutfabad — eight d.ays on camels; (-2) via
Shahidii to MeUua— 120 wiles ; (3) via siiohidli to Fort Cherkeshli
and Meshed, — for 85 miles between the Murghab .ind Tejeud there
is scarcolv any water; (4) via Sarakhs to Jlcshed, 9 or 10 marches
for camels, and, according to Petrusevitch, without water between
Merv and Sarakhs — 120 miles.
To the Afghan frontier lead (1) the track via Sarakhs and up the
Heri-rud to Herat — fit for a coach, according to Sir Charles Mao-
Gregor and Mr Lessar ; and (2) a practicable track, used by Abbott
and Shakespear, up the Murghab and Kiishk rivers.
To tlio Oxus in Bokharian tenitoiy lead several tracks, the
chief of wliich is that to Charjui — nine marches for camels. Water
is scarce.
To Khiva by the direct track is 360 miles. Water is scarce.
Population. — The Turcomans, according to Sir Heniy Kawliuson
and otliers, are descendants of the Ghiiz or Komani, a race of Twrks
who migrated westward from their homes in the Altai before the
Christian era, and penetrated even to the Danube. From sub.
sequent intermixture with Persian and Caucasian peoples, they
exhibit variations from the true Tartar tj-pe. According to Baron
de Bode the Turconi.in closely resembles both in appearance and
in speech the Nogai Tartar and the Tartar of Kasan en the Volga.
They are an independent race, as wild and free as their native
desert, brave and very impatient of control — "Wild warriors in
stormy freedom bred '' (Moore). They have a very evil reputation
for brigandage and murder, so much so that the Bokhaiaana and
Kluvans have a proverb — "IE you meet a viper and a Mervi, com-
mence by killing the Merri and then despatch the viper." Of late
years a change for the better has- taken place, and recent travellers
among them state that the Mervis show an inclination to lead a
more settled life and to establish aa elementary form of governmcu".
(Medjliss), and that it is no longer accounted an honour amoug
them to kill their neighbours. Opium smoking and arrack drink-
ing are apparently widespread vices (O'Donovan); at the same time
thCT are described as clever and intelligent
The Merv Tekkes (like the Akhal Tekkes) are classed in two great
divisions — the Toktamish and the Otaniish. Each of these
divisions consists of two clans, and each clan is subdivided into
families. The two clans of the Toktamish are called Beg and
Wakil ; those of the Otamish, Suchmuz and Bukshi. The clans oi
Beg and Wakil are the most powerful, and occupy that part of the
oasis which lies on the right or east bank of the Murgnab. The
Suchmuz and Bukshi have their tents on the left or west bank.
There is no machinery of government, and no taxes ar« levied.
Whatever government there oe is of a patriarchal nature. Each
family has a ketkhoda (patriarch), who represents the family in
matters of policy, but can only act in accordance with the wishes
of the clan. The aJcsakah, or grey beards, are also useful in settling
intertribal disputes, but they are tolerated only so long as they do
not aqt in opposition to the tribesmen. For external affairs and in
time of war the kclkhodas exercise a certain amount of power. The
authority of ketkhodas and aksakals is, however, overriden by the
laws of custom or usage (deb) and the less respected laws of religion.
The injunctions of deb are paramount It sanctions the alamaii,
or plundering raid, and in general regulates the Turcoman's daily
life ; its prescriptions are- more binding than those of the Koran.
The Tekkes marry young. The fattier purchases for his twelve-
year-old son a child-wife for 600 to 2000 loans (£20 to £80). A
young widow cf twenty-fiv^ is mnch more valuable, but a woman
over forty is not worth the price of a camel. On the conclusion ol
the bargain, the priest reads a prayer from the Koran, and the
marriage becomes valid.
The dress of the men consists of a long tunic of coarse crimson
silk reaching below the knees, with a white sash through which is
stuck a dagger ; an outer robe of brown camel-hair cloth, a huge
sheepskin hat, trousers and slippers or amber-coloured knee-boots,
complete the costume. The women are exceedingly fond of trinkets,
rings, and amulets, which accompany their movements with a
sound as it were of bells. Their dress consists of the same red silk
robe as the men wear, with a sash round the waist and high-heeled
boots, red or yellow.
The religion is Suni Mohammedan : their language Jagatai or
Oriental Turk.
The numbera of Merv Tekkes on the Murghab and Tejend are
variously estimated, but may be stated approximately at 40,000
tents, including 5000 tents of the Salor tribe. These 40,000 tents
represent a population of 200,000 to ^50,000 souls. The Salorsand
Sariks at Yulutan and Panjdeh, higher up the Morghab, are given
at 11,000 tents, or some 60,000 sonls.
Produeta, Arts, and Manufaciurcs. — 'Hic country in all times has
been renowned throughout the East for its fertility. Strabo telle us
"that it was not nncommon to meet with a vine whose stock could
hardly be clasped by two men with outstretched arms, whil<>
44
M E _R — M E R
clusters 6f Rrapos ini''lit 1)C gatlieriil two cubits in length." The
Arab traveller Ibii Hauk.il, writing in the 10th teutury, vemarks
that " tho fruiti of Merv are lintr thim thosK of any other place, and
one cannot see. in any other city such palaces with groves and
streams and gardens." ., A local proverb says, "Sow a grain to
reap a hundred. ^All cereals and many fruits grow in great abund-
Tlie Turcomans pos*ss a famous breed of horses,— not prepos-
sessing' in appearance, being somewhat le"gy and long in the back
and neck, but capable of accomplishing long distances— 50 or 60
miles — for several days in succession, and with very little food.
Thi>ir great peculiarity appears to be their hiirlessness ; the coat is
very fine, the mane and tail very scanty. This breed of horses, as
well as the wealth of the Jlerv Tekkes in camels and flocks, is fast
disappearing
The Turcomans are noted as excellent workers in silver and as
armourers, and their carpets arc superior to Tersiau. Tliey also
make felts and a rough cloth of sheep's wooh
One of tlio chief occupations of the male .sex is the repair of the
dams and the clearing of the c;inals, upon the efficiency of which
tlieir existence is dcfcndent. The services of a large number of
workmen are always held in readiness for the purpose. In 1878
the unusual roass of *ater in the Murghab carried away the dam,
and the drying up of some of the canals nearly led to a failure of
the crops.
CTinuite.— The position of Mcrv, in tho niidst of sandj deserts in
the heart of Asia, makes tho climate in the heat of summer most'
0]ipiessive. The least wind raises clouds of fine sand and dust,
which fill the air, render it so opaque as to obscure the noonday sun,
and make respiration difficult. In winter the climate is very fine.
Snow falls rarely, and melts at once.
History. — The name Jlerv, or some similar form, occurs at a
very early period in the history of the Aryan race. Under Mmiru
we find it mentioned with Bakhdi (Balkh) in the geography of the
Zend Avesta {Fcndklad, fargand i., ed. Spiegel), which dates prob-
ably from a period anterior to the conquest of Bactria by the
Assyiians, aud therefore at least one thousand two hundred years
before the Christian era. Under the name of Margu it occurs in the
cuneiform inscriptions of Darius Hystaspis, where it is referred to as
forming part of one of the satrapies of the ancient Persian empire
{Inscriptimcs Echisiatii, ed. Eossowicz). It afterwards became a pro-
vince {Mapymi/^) of the Gricco-Syr.-an, Parthian, and Persian king-
doms. On the Jlargus- the Epavdus of Arrian and now the llurghab
—stood the capital of the district, Antiochia Margiana, so called after
.\ntiochns Soter, who rebuilt the city founded by Alexander the
Great. About the 5th century, during tho dynasty of the Sasa-
nids, Merv was the seat of a Christian archbishopric of the
Nestoiian Church. In the middle of tho 7th century the flood of
Arab conquest swept over the mountains of Persia to the deserts of
Central Asia. Mcrv waa occupied 668 a.d. by the lieutenauts of
the caliph OLhman, aud was constituted the capital of Khorasan.
From this city as their base the Arabs, under Kuteibe bin Jluslim,
early in the Stli century brought under subjection Balkh, Bokhara,
Fer"hana, and Kashgaria, and ]>cnetrated into China as. far as the
province of Kan-su, In tho latter part of the 8th century -Merv
became obnoxious to Islam as the centre of heretical propaganda
preached by Jlokaunah (Hascheni ben Hakem), tho "veiled
prophet of khorasan," who claimed to be the incarnation of the
Pfity. In 874 Arab rule in Central Asia came to an end. Dur-
in" their dominion Merv, like Samarkand aud Bokhara, became
on'o of the gi-eat schools of science, and the celebrated historian
Yakut studied iu its libraries. About 1037 the SSljukian Turks
crossed the Oxus from the north and raised Toghrul Beg, grandson
of Seljuk, to the throne of Pereia, founSing the Seljukian dynasty,
with its capital at Nishapur. A younger brother of Toghrul,
Daoud, took possession of llerv and Herat. Toghrul was succeeded
by the knowued Alp Arslan (the great lion), whose sway was so
vast that, according to tradititn, no fewer than twelve hundred
kii>gs princes, and sons of kings and princes did homage before
his throne. Alp Arslan was buried at Merv. It was about this
time that Merv reached tlie zenith of her glory. During the reigii
of Sultan Sanjar of tho s.ime house, towards tho middle of the llth
century, Merv was overrun by the Turcomans of Ghuz, and tho
country was reduced to a state of misery and desolation. These
Turcomans, tho ancestors of tho present tribes of Turcomania,
were probably introduced into the country by the Seljukian Turks
as niiiitai-y colonists. They formed the van of their armies, and
rendered efficient service so long as the dynasty lasted, and after-
wards took part in the wars of Tamerlane.
In 1221 llerv opened its gates to Toulai, eon of Jenghiz, khan
ot the Mongols, on which occasion the inhabitants, to the number
of 700 000, are said, to have been butchered. From this time
fgnvarii Merv, which had been the chief city of Khorasan, and
was popularly supposed to contain a million inhabitants, com-
menced to languish in obscurity. In tho early part of the 14th
century Merv w.ts again tho seat of a Christian archbisho]iric of the
ILastern Church, a On thu death of the grandson of Jengliiz lihan
Mei^v became included in the possessions of Toghluk Tiifaur !Uiaq
Cl'amerlane), in 13S0. In 1505 the decayed city was occupied bj
the Uzbeks, who five ycara later were expelled by Ismail Khairj
the founder of the Suffavcan dynasty of Persia.''^ Merv thencefo-J
ward remained in the hands of Persia nutil 1787, when it waf
attacked and captured by the emir of Bokhara.'^ Seven yean
later the Bokhanans razed the city to the ground, broke down the
dams, and converted the district into a waste. About 1790 tha
Sarik Turcomans pitched their tents there. When Sir AlexanSec
Burncs traversed the country in 1832, the Khivans were the nilers
of Merv," the nomad population being subject to them. About this
time the Tekke Turcomans, then living at Ora2kala on the Heri-nid,
were forced to migrate northwaid in consequence of the pi-essui*
from behind of the Persians. The Khivans contq»ted the advance
of the Tekkes, but ultimately, about the year 1856, the latter be-
came the sovereign power in the country, and' have tver.BJuce
resisted all attempts at reconquest
.4«f/i(jn'/iM.— Besides the 8tandai-d travels of Wolff, Fen-ler. Vamlicry, Burnet;
Abbott, ilomnvleff, and others, the foUirwiiig works and papers of more recent
diile may be consulted with advantaRc :— Sir H. Rawhnson's En^fand and RvttiM
in the- £ast; O'Donovan'a correspondence with the Z>ot/j/ yetca, 1880-Sl;
O'Donovan's -'Merv," Proc. Roy. Oeo^. Soc; Col. Stewart's "Ci.unTy of the
Tekke Turcomans." /•roc. Itot/. Oco<j. Soc, with excellent map ; " 1 he New Ruaso-'
Persian Frontier, 1881." Pi-oc. liotj. Geog. Sec.', Glrard de Itlallc, il^otre tur
tAsie Cenlrale; Sir II. Rawliiison, "Road to Merv," Proc. Itoi/. Geoff. Soc;
Col. Baker's clouds in the Etul\ Captain Napier's •- Repoi-ts," jQ-ui\ Ron. Oeog.
Soe.; Iluttpn's Central Atia; Marvin's Hern; Col Potto's Steppe Campaignt;
Sir Charles MucGregof'B Journey fhrmtgh Khorassan ; Boulger'B England and
Russia in Central Asia ; Captain Dutler's Communications to the Public Preui
l.ossav'a " Journeys," Pfoc. Roy. Oeog. Soc. ; O'Donovan's Merv Oasis ; PapeiBtm
t lie Turcomans, ic, by CoL Petrnsevltch, Proc. Imp. P.uss. ileog. Hoc. Csdcosiu
SLCIlon; Col. GrodckofTs Journey from Tashkend to Persia, 1S80; Captain
Knropiitkln's Turcomania, 1830; Col. VenlukofTs Progress of Russia in Central
Asia, 1877, and other papers by the same author ; Col- Kostenko's "Turkestan,"
Jour. R. U. S Instn. ; Schuyler's Turkislon ; coirespoiHience on Central Asia prt-
se.itfid to parliament, Jtc. . iV. C. H. Ci
MERYON, Charles (1821-1868).. The name' o!
M^ryon is as.sociated ■with that spiriteti revival of etching
in France which took place in the middle of the 19th
century, — say from 1850 to 1865, — but it is rather by the
individuality of his cwn achievements, and the strength of
llis artistic nature, than by the influence he exercrsed-that
M^ryon best deserves fame. No doubt His -syork encouraged
others to employ the same medium of expression, and s»
great was his own perfection of technirjue that he may well
have been made a model ; but, after all, the medium he
selected, and in which he excelled, was but the accident of
his art ; he was driven to it in part by stress of circum-i
stances — by colour blindness ; and, even with colour blind-
ness, his extraordinary certainty of hand and his delicate
perception of light, aided by his potent imagination, would
have made him a great draughtsman not alone upon the
copper.
Charles M^ryon was born in Paris in 1821. His fathei
■n'as an English physician, hia mother a French dancer.
It was to his mother's care that M^ryon's childhood 'waa
confided. She was supplied with money, and she gave the
boy passionate afifection, if not a -wise training. But she
died -when he was still very young, and !M(?ryon in due
time entered the French na-vy, and in the corvette "L«
Rhin " made tho voyage round the world. He was already,
a draughtsman, for on the coast of New Zealand he mads
pencil drawings which he was able to employ, years after-
wards, as studies for etchings of the landscape of those'
regions. The artistic instinct developed, and, while ha'
was yet a lieutenant, JWryon left the nav)'. Finding that
he was colour-blind, MiSryon determined to devote himself^
to etching. He entered the work-room of one Bli5ry, from'
whom he learnt something of technical niatters, and to
whom ho always remained grateful. M^ryon was by this
time poor. It is said that he might have had assistance
from his kindred, but he was too proud to ask it. And
thus he was reduced to the need of executing for the sake
of daily bread much work that was wholly mechanical and
irksome.. Resolutely, though unwillingly, he became the
hack of his art, doing frequently, from the. day when he
waa first a master of it to the day when insanity disabled
him, many dull commissions which paid ill, but Jiaid better^
than his original works. *• Among learner's work,* done foi]
his own adwintage, are to be counted somastudies after. the
MiEiS — M E S
45
Dutch etchers siich as Zeeman and Adrian van de Velde.
Having proved himself a surprising copyist, he proceeded
to labour of his own, and began that series of etchings
which are the greatest embodiments of his greatest con-
ceptions— the series called " Eaux-fortes sur Paris." These
plates, executed from 1850 to 1854, are. never to be met
with as -a set ; they were never expressly published as a
set. But they none the less constituted in M6ryon's mind
an harmonious series. For him their likenesses and their
contrasts were alike studied ; they had a beginning and an
end ; and their differences were lost in their unity.
Besides the twenty-two etchings " sur Paris " character-
ized below, M^ryon did seventy-two etchings of one sort
and another, — ninety-four in all being catalogued in
Wedmore's Meryon and Meryon's Paris ; but these include
the works of his apprenticeship and of his decline, adroit
copies in which his best success was in the sinking of his
own individuality, and dull and worthless portraits chiefly
of forgotten celebrities. Yet among the seventy-two prints
outside his professed series there are at least a dozen that
will aid his fame. Three or four beautiful etchings of
Paris do not belong to the series at all. Two or three
etchings, again, are devoted to the illustration of
Bourges, a city in which the old wooden houses were
K attractive to him for their own sakes as were the stone-
built monuments of Paris, But generally it was wlien
Paris engaged him' that he succeeded the most. He
would have done more work, however, — though he could
hardly have done better work,— if the material difficulties
of his life had not pressed upon him and shortened his
days. He was a bachelor, unhappy in love, aiid yet, it is
related, almost as constantly occupied with love as with
work. The depth of his imagination and the surprising
mastery which he achieved almost from the beginning in
the technicalities of his craft were appreciated only by a
few artists, critics, and connoisseurs, and he could not sell
his etchings, or could sell them only for about lOd. a piece.
The fact that his own origiRal work was of incalculably
greater value than his best copies of his most celebrated
forerunners had not yet impressed itself upon anybody.
Disappointment told upon him, and, frugal as was his way
of life, poverty must have told on him. He became subject
to hallucinations. Enemies, he said, waited for him at the
corners of the streets ; his few friends robbed him or owed
him that- which they would never pay. A very few years
after the completion of his Paris series, he was lodged in
the madhouse of Charenton. Its order and care restored
him for a w-hile to heal,th, and he came out and did a little
more work, but at bottom he was exhausted. In 1867
he returned to his asylum, and died there in 18G8. In the
middle years of his life, just before he was placed under con-
finement, he was much associated with Bracquemond and
with Flameng, — skilled practitioners of etching) while he
was himself an undeniable genius, — and the best of tlie
portraits we have of him is that one by Bracquemond
under which the sitter wrote that it represented " the
sombre Meryon with the grotesque visage." And it did.
There arc twenty-two pieces in the Eaux-fortes sur Paris. Some
of them are insignificant. That is because ten outof tlie twenty-
two were destined as headpiece, tailpiece, or running conimeutJiry
on some more important plate. But eacli lias its value, and certain
of the smaller pieces throw great light ou the aim of the entire set.
Thus, one little plate— not a picture at all— i.s devoted to the record
of verses made by Meryon, the purpose of which is to lament the life
of Paris. The misery and poverty of the town Meryon had to illus-
trate, as well as its splendour. The art of Meryon is completely
misconceived when his etchingsare spoken of asviewsof Paris. They
arc often "views," but they ai-e so just so far as is compatible with
their being likewise the visions of a poet and the compositions of an
artist. It was an epic of Paiis that Jleryon determined to make,
tibloured strongly by his personal sentiment, and affected hero and
there by the occurrences of the moment, — in more than one case, for
instance, he hurried with p>>.rticular affectioa to etch his impression
of some old-world building which was ou the point of ilestnu'tion.
Nearly every etching in tiic series is au instance of technical skill,
but even the technical skill is e.wrcised most happily in those etch-
ings whicTi have the advantage of impressive subjects, and which
the collector willingly chcrislies for their mysterious snggestiveuess
or for their pure beauty. Of these, the AWide de Koir« Danit is
the general favourite ; it is commonly held to be Meryon's master-
piece. Light and shade play wonderfully over the gieat fabric of
the church, seen over the spaces of tlie river. As a draughtsman of
architecture, Meryon was complete ; his sympathy with its various
styles was broad, and his work ou its various styles unbiassed and
of equal perfection— a point in which it is curious to contrast him
with Turner, who, in drawing Gothic, often drew it with want of
appreciation. It is evident that architecture must enter lav:,'ely
into any representation of a city, however much such represeutatioii
may be a vision, and however little a chronicle. Besides, the archi-
tectural portion even of Meryon's labour is but indirectly imaoiua-
tivc ; to the imagination he has given freer play in his dealin'rs'with
the figure, whether the people of the street or of the river°or the
people who, when ha is most frankly or even wildly symbolical,
crowd the sky. Generally speaking, his figures are, as regards
draughtsmanship, " landscape-painter's figures." They are drawn
more with an eye to grace than to correctness. But they are not
" landscape-painter's figures " at all when what we are concerned
with is not the method of their representation but the purpose of
their introduction. They are seen then to be in exceptional accord
with the sentiment of the scene. Sometimes, as in the c.ise of La
Morgue, it is they who tell the story of the picture. Sometimes, as
in the case of La Rue des Mauvais Carbons, — with the two pa.ssing
women bent together in secret converse, — they at least suggest it!
And sometimes, as in L'Arche du Pont Notre Dame, it is their
expressive gesture and eager action that give vitality and animation
to the scene. Dealing perfectly with architecture, and perfectly, as
far as concerned hiq peculiar purpose, with humanity in his art,
Meryon was little called upon by the character of his subjects to
deal with Nature. He drew trees but badly, never representing
foliage happily, either in detail or in mass. But to render the char-
acteristics of the city, it was necessaiy that he should know how to
pourtr.-iy a certain kind of water — river- water, mostly sluggish — and
a certain kind of sky— the grey obscured and lower sky that broods
over a world of roof and chimney. This water and this sky Merj-on
is thoroughly master of ; he notes with observant affection their
changes in all lights.
iteryou's excellent draugiiiinanship.and his keen appreciation"of
liglit, shade, and tone, were, of course, helps to his becoming a great'
etcher. But a living authority, himself an eminent etcher, and
admiring Meryon thoroughly, has called Meryon by preference a
great original engraver,- so little of Meiyon's work accords with Mr
Hadcn's view of etching. Sliryon was anything but a brilliant
sketcher; and, if an artist's success in etching is to be gauged cliieflv
by the rapidity with which he records an impression, Meiyon's suo
cess was not great. There can be no doubt that his work was
laborious and deliberate, instead of swift and impulsive, and that of
some other virtues of the etcher — "selection" and "abstraction" SB
Mr Hamerton has defined them — he shows small trace. But a
genius like Meryon is a law unto himself, or rather in his practice
of his art he makes the laws by which that art and he are to be
judged. He was a great etcher, and by his most elaborate labour
he seemed somehow to ensure the more completely for bis picture
that virtue of unity of impression which, it may well be admitted,
oftener belongs to rapid than to deliberate work. In Meryon's
etchings the hand-work never seems tg be in arrear of the thought
As long as the hand-work must continue, the thought and passion
are retained. Meryon knows the secrets of his craft as well as did
the older masters of it ; but he turns them to his own purposes.
He is unexcelled in strength and in precision, nor is he often
rivalled in delicacy. These qualities,- and othcre more distinctly
tecbnic.ll, which it would take too long to insist on here, students
find in his etchings. But the incommunicable charm of Meryon's
prints and their lasting fascination are due to the fact that, behind
all technical qualities, and as their veiy source and spring, there
lies the potent imagination of the artist, poetical and vivid, direct-
ing him what to see in his subject, and how to see it. (F. WE.)
MESCHERYAKS, or Meschers, a people inhabiting
eastern Russia. Nestor regarded them as Finns, and
even now part of the Mordvinians (of Finnish origin)
call themselves Meschers. Klaproth, on the other hand,
supposed they were a mixture of Finns and Turks, and the
Hungarian traveller Reguli discovered that the Tartarized
Meschers of the Obi closely resembled Hungarians.- They
formerly occupied the basin of Jhe Oka (where the town
Meschersk, now Meschovsk, has maintained their name)
and of the Sura, extending north-cast to the Volga. After
the conquest of the Kazan empire by Russia,.^partl.Df
46
M E S — M E !S
them migrated north-eastwards to the basins of the Kama
and Byelaya, and thus the Meschers divided into two
branches. The western branch became Russified, so that
the Mescheryaks of the governments of Penza, Saratoff,
Ryazan, and Vladimir have adopted the customs, language,
and religion of the conquering race; but their ethnogra-
phical characteristics can Ije easily distinguished in the
Russian population of the governments of Penza and
Tamboff. The eastern branch has taken on the customs,
language, and religion of Bashkirs, with whom their fusion
is still more complete. They can be distinguished from
their neighbours only by their more peaceful character.
This Bashkir-Mescheryak branch was estimated by Rittich
in 1875 to number 138,000. They make 6 per cent, of
the population of the government of Upa, and 22 per
cent, in the district of Birsk. The number of the western
Mescheryaks is unknown, and could hardly be estimated on
account of their mixture vnth Russians. It is only in the
government of Penza that they have maintained theirnational
features ; there they make 3 per cent, of the population.
MESCHOVSK, a district town of Russia, in the govern-
ment of Kaluga, 45 miles to the south-west of the capital
of the province. It is an old town supposed to date from
the 13th century, and it is often mentioned in Russian
annals under the names of Mezetsk, Mezechevsk, or
Meschorsk. About the end of the 14th century it was
embraced in Lithuania, and it was ceded to the Moscow
" great principality " in 1 494. It was often pillaged by Tar-
tars in the 1 6th century, and during the great distm-bances
of 1610 all its inhabitants were killed by the Zaporoghi
Cossacks, and the fort was taken by Poles, who returned it
to Russia only after tha treaty of Deulm. The country
round Meschovsk is not fertile ; but, from its position on
old established routes to the south, the to^vn has become
a centre of considerable trade. Its annual fair, which
takes place on the grounds of the very old Petrovsk
monastery, is important to the surrounding districts for
the export sale of horses,, grain, hemp, hempseed oil, and
coarse linen, and for the import trade in cottons, woollens,
and earthen and glass wares, the whole turn-over reaching
about £100,000. Population, 7400.
MESHED (properly Mesh-hed, i.e., "place of martyi;;
dom," "shrine"), a city of northern Persia, capital of
Khoriisiin, 472 miles east of TehrAn, 201 miles north-west
of Herat, 36' 17' 40" N., 52° 35' 29" E., lies on a plain
watered by the Keshaf-rild, a tributary of the Heri-rud, and
is surrounded by mud walls 4 mUes in circumference, with
a dry ditch 40 feet deep at some points, which could be
flooded from the neighbouring reservoir and watercourses.
Within this enclosure is a strong citadel, with good walls 25
feet high, residence of the prince governor of KhorAsAn.
There are five gates, from one of which, the Bala KhlabAn,
the KhiabAn main street runs right through the city, form-
ing a fine boulevard planted with plane and mulberry trees,
and with a stream of dirty water running down its whole
length. In the centre is an open parallelogram 160 yards
by 75, encircled by double-storied cloisters, and pierced on
the long side by a high arched porch leading directly to
the great mosque, whose gilded dome ri.ses al>ove the .shrine
of the famous ImAm RizA.' The marble tomb of the .saint,
• 'AH Ri?a (or el-Rida), the eighth imnm of the Rhi'a, is the 'Ah' ihn
Miisi from whom the party of Alides h.id sucli liopcs under the
caliphate of Mamun (see Siohammedanism). Ho died at fiia,
818 A.D., and was buried by Mamun's orders in the vicinity of tliat
town beside the grave of Hariin el-Rash{d. To the Alides he was a
martyr, being believed to have been poisoned by the caliph, Ibn Batutn,
who describes both shrines (iii. 77 sq.), tells how the pious visitors
to the slirine of 'Ali ibn Mi'isd used to spurn witli tlieir feet the tomb
of Rashfd. In Ids time a considerable town had been formed around
the shrink uiider the name of Moshhed el-Rid.i and uUiiiiatcIy llie
now town eclipsed the older city of Tus.
which is the most venerated spot in the whole of Persia,
and yearly visited by from 80,000 to 100,000 pilgrims, is
surrounded by a silver railing, and approached by a flight
of inlaid marble steps. Eastwick, the only European before
O'Donovan who penetrated as far as the parallelogram,
describes the mosque as large enough to contain three
thousand people. It is flanked by two gilded minarets,
one of which, 120 feet high, is e.^ttremely beaiitiful, with
an exquisitely carved capital, built by ShAh AbbAs. The
fa9ade is entirely covered with blue and white enamelled
tiles. To the mosque are attached as many as two thoasand
attendants and retainers of all sorts, including no less than
five hundred mollahs. Beyond the dome is Gauhar ShAh's
handsome mosque, surmounted by an immense Mue dome,i
and also flanked by two minarets. In the main street
is a public kitchen supported by the enormous revenues
of the. shrine, where eight hundred devotees are daily,
supplied with food gratuitously. The only other notable
buildings in the place are some colleges and twenty-'
two caravanserais, one of which is of great size. Meshed
does a considerable local and transit trade to the yearly
value of about 600,000 tomans, and its bazaars are always
well stocked with silks, velvets, felts, cottons, shawls,'
carpets, lacquer work, lambskins, hai'dware, glass, chica,]
and other goods from South Persia, India, Turkestan, and
Russia. The European trade is now entirely controlled by
Russia, and European manufactured articles are mostly all
from that country. The chief manufactures are silk, satin,
velvet, and checked-cotton fabrics, carpets, shawls, noted
sword blades, shagreen, and turquois jewellery. Within
the enclosures are extensive cemeteries far exceeding the
local requirements, large numbers of the faithful being
brought from all parts of the Shi'a world to be buried in
the vicinity of RLzA's shrine under the belief that their,
eternal salvation is thereby ensured.
Some 10 miles west of Meshed is a powder factory, formerly
under Colonel Dolmago, where powder of- excellent quality is p«K
duced. The district, although fertile, does not produce sufficient
for the inhabitants, so that much grain has to be imported from
Kurdistan and Nislidpur. The climate is very severe iu winter, with
much snow ; in summer it is less sultry than might be expected,
the temperature ranging from 76" F. to 90° or 92° F., and in excep-
tional years 94° to 98° F. The population is variously estimated at
from 45,000 (Connolly) and S0,000 (Ferrier) to 80,000 and 100,000
(Eastwick). The settled residents, exclusive of pilgrims and foreign
traders, are estimated by O'Donovan at 50,000. ",
The main caravan routes from Khiva, Bokhara, Samarkand, and
Herat converge at Meshed, whence lines of traffic radiate to Kuchan
for the Atrek valley and the Cas]iian, to Nishapur and Bostara for
Tehran, to Tahas for Isfalidn, to lihat for Sistan and Kirrodn. It
thus occupies a position in north-eastern Persia analogous to that
of Tabriz iu the north-west.
MESHED-ALI, i.e., the shrine of the " martyr " Ali, is
a town of Asiatic Turkey, province of Baghdad, 50 miles
south of Kerbela, close to the ruins of Kufa, and 2 miles
west of the Hindlye branch of the Euphrates, the reputed
burial-place of the caliph Ali.- It stands on the east
scarp of the Syrian desert, and is enclosed by nearly square
brick walls flanked by massive round towers dating from
the time of the caliphs. Under the gilded dome of the
great mosque, which occupies the centre of the town, is the
shrine of Ali, which is held by the Shi'a as at least as
holy as the Kaaba itself. Any Moslem buried within
siglit of the dome being certain of salvation, large numbers
of bodies are yearly- sent from all parts for interment here.
Besides the mosque M'ith its richly decorated facade, the
only noteworthy building is a good bazaar su])plied from
Baghdad and Basra. The to^vn itself, whicli Lady Anne
^ Wliether the place really contains the grave of Ah was long
disputed, and the story given in defence of its claims is doubtless
apocryphal. The dome was built under the Abbasids, and the resting-
place of the caliph \>n!;uuv,n or concealed under the Oniayyads (Ibn
Haukal, p: 163).
M E S — M E S
47
Blunt describes as " an ideal Eastern city, standing in an
absolute desert, and bare of all surroundings but its tombs,"
consists of narrow gloomy streets lined by houses closely
packed together. The locality is properly named Najaf,
and gives its name to the neighbouring lake, a large
depression filled by an eruption of the river, and ranging
from 6 to 20 feet in depth. The accumidated treasures
of the shrine were carried ofE by the Wahhiibites when they
captured this place early in the present century. The
population is estimated at 7000, including several Indian
Mohammedans under the protection of the British resident
at Baghdad.
The asiiect of the shrine in the 14th century is doscribej by Ibn
Batiita, i. iH sq. A plan of the town and description of its
splendour before the Wahhabites pillaged it is given Dy Niebuhi-.
See also Ibn Jubair, p. 214 ; P. Teiieira, /(in., cap, iv.
MESHED HOSEIN, properly Meshhed Hosein. See
Keebela, vol. xiv. p. 48.
MESilER, MESMERISM. See vol. xv. p. 277.
See Plata MESOPOTAMIA, the " country between the rivers," is-a
"111. 'purely geographical expression, the countries which it com-
prehends never having formed a self-contained political
unity.' It was first introduced by the Greeks at or after
the time of Alexander, but probably had its origin in the
earlier Aramaain name letli naJirtn (the country between the
rivers), to which again corresponds the Biblical Aram N^aka-
rayim.^ As early as 700 b.c. " the country of two rivers "
is mentioned on the Egyptian moniunents under the name
?Taharina, but no such designation appears in the cimei-
form inscriptions (though the territory formed part of the
Assyrian as it afterwards did of the Persian empire). The
most settled period in the history of Mesopotamia was
probably under Persian-Greek rule. Xenophon applies
the name Syria to the extremely fertile district which he
traversed after having crossed the Euphrates at Thapsacu.s.
The country beyond the Araxes (Chaboras ?) he calls Arabia,
— a desert region in which his army had to suffer great
hardships until it reached the " gJltes of Arabia." Even
in later times Mesopotamia was included under the name
Assyria, or was reckoned part of Babylonia.
These statements of Xenophon already indicate a
demarcation of the territory afterwards called Mesopotamia,
as well as its division into two sections. The fertile
portion, inhabited by agricultural Aramaeans, stretched
from the Euphrates to the Chaboras ; the desert portion,
the home of wandering tribes, extended to the Tigris. It
would be rash, however, to conclude from this that
Mesopotamia designated the whole territory between the
Euphrates and Tigris ; indeed it is -possible that Aram
Najiarayim, the Aram of the country of the two rivers,
originally meant only the main portion of the fertile country
inhabited by Syrians. In this case the two boundary
rivers must have been, not the Euphrates and the Tigris,
but the Euphrates and tl\e Chaboras. After the final
occupation of the country by the Romans (156 a.d.), the
political province of Mesopotamia was practically confined
to this more limited district. Though in ordinary usage
»the Euphrates and Tigris are considered as the two rivers
• which bound 'Mesopotamia, the one bank of the river
cannot be geographically separated from the other, and
consequently narrow strips of country on the right bank
of the Euphrates and on the left bank of the Tigris must
be reckoned to the country "between" the rivers. On
the other hand, the country between the sources of the
Euphrates and the Tigris has from early times • been
* Mcffoirora/iio, more exactly ^ ^etni tatv TroTofiwyt soil. x^P"^
or Zvpfa. ' -■'-.fj.,,.- •.
Jt In the more recent parts of Genesis Padan Aram takes tbe place
of Aram Naharayini. Bnt this perhaps is the name of a smaller district
in the neighbourhood of Harran. '
reckoned not to Mesopotamia but to Armenia. In this
direction the Masius range forms the proper boundarj-, and
it is only on rare occasions ,that theoretical geographers
extend the name Mesopotamia over the more northern
districts, Sophene, &c. Purely theoretical too, and not to
be approved, is the extension of the definition so as to
include the land of Babylonia ('IrAk 'Arabi), that is, the
country as far south as the confluence of the Euphrates
and Tigris, or even as far as their embouchure in the
Persian Gulf.
From what has been said it appears that Mesopotamia
reaches itsnorthern limitsat the points where theEuPHBATES
(?.!'.) and the Tigris break through the mountain range and
enter the lowlands. In the case of the Euphrates this
takes place at Sumeisdt (Samosata), in that of the Tigris
near Jezlret ibn 'Omar (Bezabdd) and Mosul (Xineveh).
Consequently the irregular northern boundaries aru marked
by the lowland limits of those spurs of the Taurus mountains
known in antiquity as Mons Masius and now as Karaje
DAgh and Tur "Abdin. Towards the south the ancient
boundary was the so-called Median WaU, which, near
Pirux Shapur, not much to the south of Hit (the ancient
Is), crossed from the Euphrates in the dii-ection of Kadisiya
(Opis) to the Tigris. There the two rivers approach each
other, to diverge again lower down. At the same place
begins the network of canals connecting the two rivers
which rendered the country of Babylonia one of the richest
in the world ; there too, in a geological sense, the higher
portion of the iilain, consisting of strata of gypsum and
marl, comes to an end ; there at one time ran the line of
the sea-coast ; and there begin those alluvial formations
with which the mighty rivers in the course of long ages
have filled up this depressed area. Mesopotamia thus
forms a triangle lying in the north-west and south-east
direction, with its long sides towards the north and south-
west. It extends from 37° 30' to about 33° N. lat. and
from 38° to 46° E. long., and has an area of some 55,200
square miles. The points at which the rivers issue from-
among the mountains have an absolute altitude of between
1000 and 1150 feet, and the plain sinks rapidly towards
the southern extremity of Mesopotamia, where it, is not more
than about 1G5 feet above the sea. As a whole the entire
country consists of a single open stretch, save that in the
north there are some branches of the Taurus — the Nimnid
DAgh near Orfd, the long limestone range of 'Abd-el'Azlz,
running north-north-west, and farther to the' east the Sinjar
range, abo of limestone, 7 miles broad and 50 mUes long,
running north-northreast. Between these two ranges — near
the isolated basaltic hill of Tell K6kab (Hill of Stars) — runs
the defile by which the waters of the Chaboras, swollen
by the Jaghjagha and other affluents from the Masius, find
their way into the heart of Mesopotamia. The KhAbiir
proper, the ancient Chabora.s, which rises in the three-
hundred copious fountains of RAs- ain (the ancient Bhesaena),
and ultimately falls into the Euphrates near KarkisiyA
(Circesium), forms the boundary between the two, or mora
correctly the three, great divisions of Mesopotamia. ■, These
divisions are (1) the northern country to the west of the
KhAbTir, (2) the northern country to the east, and (3) the
steppe-land. In the country to the north-west of the
KhAbiir we must probably, as already mentioned, recognize
the true ancient Aram Naliarayim. Under the dominion
of the Seleucids it bore the name of Osrhoene, or better
Orrhoene, and was for a time the seat of a special dynasty
•which at a later date at any rate .was Arabian (Abgar).
The capital of this kingdom was Orfa (Roha), the Edessa
of the Greeks and Romans, the Orrhoi of the Syrians ; it
was at a later date a Roman colony, and bore also the name
of Justinopolis. This once flourishing city lies on the small
river Daisan (the ancient Scirtus). South of Edessa lie
48
MESOPOTAJIIA
the ruins of Hajiran (see vol. xi. p. 454). In the Mongolian
period Harran fell into decay, and at present it is a mere
heap of ruins. A third tflwn of this region is Serug
(Gen. xi. 20) ; in the Greek period it was called Batne, but
the Syrians retained ihe name Serug, which is still in use
(Seriij). The town lies between Harran and the Euphrates,
in a plain to which it gives its name. On the left bank of
the Euphrates lay Aparaea (the modem Birejik), connected
with Zeugma on the other side by a bridge, and farther
south, at the mouth of the Bilechas (modem BeUk),
was the trading town and fortress Nicephorium, founded
by command of Alexander, and completed by Seleucus
Kicator, in memory of whose victory it was named.
From the emperor Leo it received the designation Leonto-
polis. The spot is bow knoiivn as Ra^ilfa (see below).
Farther up the fruitful valley of the Belik lay the town of
Ichnae (Chne). Farther south lay Circesium {Chdboras of
Ptolemy, Pkaleg of Isidor), not to be identified, as is usually
assumed, with Carcheraish ; from the tima of Diocletian
it was strongly fortified. The site is at present occupied
by a wretched place of the name Karklsiyi. Carchemish
probably lay near the bridge of Membij, the present
Kalat el-Nejm.
In ancient times a highly flourishing district must have
stretched along the river Chaboras (Khibiir) to its principal
source at RAs-'ain ("Fountain-head," Sjt. RUKaina, the
Bhesaena of Ptolemy), a to\\'n which was for some time called
Theodosiopolis, because after 380 A.D. it was extended and
embellished by Theodosius. Justinian fortified it. The
strip of completely desert country which now stretches along
the lower course of the KhAbur was called in antiquity
Gauzanitis, and corresponds to the Oozan of 2 Kings xviiL
6 (Guzana or Guzanu in the cuneiform inscriptions).
The country to the east of the upper KhAbiir is in many .
respects similar to that which has just been described. As
the watershed of the Tigris is not far distant, the Masius
range sends down into Mesopotamia only insignificant
streams, the most important being the Hermas, the
Mygdonius of the Greeks. On its banks was situated
Nisibis, the chief city of the district, which commanded
the great road at the foot of the mountains leading
through the steppe, which here from the scarcity of water
comes close up to the edge of the hills. In the old
Assyrian empire Nasibina was the seat of one of the four
great administrative ofliciaLs. In the time of the Seleucids
the site was occupied by the flourishing Greek colony of
Antiochia Mygdonia ; but the new designation, transferred
to the river and the vicinity of Nisibis from the Mace-
donian district of Mygdonia, afterwards passed out of use.
Nisibis was an important trading city, and played a great
part in the wars of the Romans against the Persians.
Captured by Lucullus, surrendered by Tigranes, recovered
by Trajan, again abandoned by Hadrian, once more occu-
pied under Lucius Verus, and strongly fortified by Severas,
it was at length raised to be the capita! of the pro^^nce,
and remained the frontier fortress of the Romans till in
the time of Jovian it was ceded to the Persians. After
the loss of Nisibis the emperor Anastasius in 507
founded to the north-west the fortress of Darse or Daras
(the modern DAril), also called Anastasiopolis, which from
the reign of Justinian, who increased its strength, remained
for a time the residence of the du-x Mesopotamia. Besides
these strongholds, many fortified posts were established
by the Byzantine empire in this district. Antoninopolis
must be mentioned as an important town ; this was
refortified by Constantino under the name of Constantia,
and has loft its ruins near Tela between Harran and Nisibis.
.Mardin too was a fortress of a similar kind, and the town
of Singara, at the southern foot of the mountain of the
same name, was an advanced post of the Roman power.
Tne south or steppe portion of Mesopotamia was from
early times the roaming-ground of AJabic tribes ; for
Xenophon gives the name of Arabia to the district on the
left bank of the Euphrates to the west of the KhAbiir-,
and elsewhere it is frequently stated that the interior at a
distance from the rivers was a steppe inhabited by Arabes
Scenitje (Tent Arabs). Along the bank of the two great
rivers ran a bolt of cultivated country, and the rocky
islands of the Euphrates were also occupied by a settled
population. On the Euphrates, beginning towards the
north, we must mention first Zaitah or Zautha, south-east
of Circesium; next Corsothe, at the mouth of the Mascash;
then Anatho or Anathan, the modem Ana ; and finally
Is (Hit). On the Tigris the point of most importance is
Cama; (Katt-ai of the Anabasis), south from the couth of
the Great Zab near the present Kal'at SherkAt ; and not
far distant towards the interior was Atrae or Hatrae, also
called Hatra, the chief town of the Arab tribe of the Atreni.
It was besieged without success by Trajan and Severus ;
by the 4th century it was already destroyed ; but the
interesting ruins, which can scarcely be visited owing to
the plundering habits of the Bedouins, still bear the name
of El-Hadhr. They lie in the heart of the steppe, and
were formerly well supplied with water.
All these districts came in G40 a.d., or pernaps a little
earlier, into the power of the Arabs, who named them
Jezfra (island) or Jeziret Akiir,' and divided them according
to tribes into three portions, the land of Bekr, of Rebi'a,
and of Modhar. The district of Modhar ran along the
side of the Euphrates, and its chief towns were Orfa and
Rakka ; the district of Rebi'a comprised the plain of
Mosul as far as the country on the KhSbiir (chief towns
Mosul and Nisibis), and the district of Bekr (Diyir Bekr)
the more mountainous country to the west of the upper
Tigris (chief town Amid or Diarbekr). In general the
Arabs consider a part of the mountain territories which lie
between the two rivers to belong to Jezira, as is best seen
from the following notice given by Abulfeda: —
"El-Jezira is the land between the Tigris and the Euphrates, yet
many places on tlie other side of the Euphrates, which properly
belong to Syria, are also included, as well as places and even dis-
tricts on the east side of the Tigris. Tlie exact boundary line thus
runs from llalatia by Sumeisat, Kal'at er-Ri'im (Eum-Kala of the
maps), and Bire (Birejik) to tho point opposite ilembij, and then
by_ Balis, Er-Rakka, Karkisiya, ErRahaba (on right bank), and
Hit to Anbar. Mere the Euphrates ceases -to form the boundary,
which runs across to the Tigris in tho direction of Tekrit, and
ascends the Tigris as far as Es-Sinn (Senna) to El-Haditha and
ilosul, thence to Jeziret ibn 'Omar, th(;n to Diarbekr, and so back to
ll.alatia."
From the Arabic geographers and travellers we gain the
impression that a great part of Mesopotamia, with the ex-
ception of the southern steppe of course, must at that time
have been in a very flourishing condition ; the neighbourhood
of Nisibis especially is celebrated as a very paradise. lu
fact it is only since the Turkish conquest of the country
under Sultan Selim in 1515 that it has turned into a desert
and gradually lost its fertility. As the nomadic Arabs
have continually extended their encroachments, agriculttire
has been forced to withdraw into the mountains ; and this
is especially true of the western portions of Mesopotamia,
the district of R.^s-'ain, and the plain of Harran and Serilj,
where huge mounds give evidence that the whole country
was once covered with towns and villages. Under the
Turks El-Jezira does not form a political unity, but be-
longs to different pashaliks.
From this brief survey it appears that Mesopotamia, like
Syria, constitutes an intermediate territory between the
great eastern and western monarchies,2=Syria inclining
Philostratus [c. 200 A,D.) already reports that the AraKs colled
MESOPOTAMIA
49i
more to the west, and Mesopotamia to the east. In
Tirtue of its position it frequently formed both the object
and the scene of contest between the. armies of those
mighty monarchies, and it is wonderful how a country so
often devastated almost always recovered. The roads, it is
true, which traversed the territory were not mere military
highways, but the main routes of traffic for Central Asia,
Western Asia, and E irope. It is only in modern times,
nnd since these lines of commercial intercourse have
ceased to be followed, that the general condition of things
has been so entirely altered.
The number of roads which in ancient times traversed
tlie country was veiy considerable ; the Euphrates formed
not a barrier but a bond between the nations on cither
side ; at many places there were at least boat-bridges
(zeugma) across. One of the most important of the
ancient crossing-places must be sought, where in fact it still
exists, at Birejik, the ancient Apamea-Zeugma. From this
point a great road led across to Edessa (Orfa) ; there it
divided into two branches, the northern going by Amid
(Diarbekr) and the otlmr by Mardin and Nisibis to Mosul
(Nineveh). lu quite recent times, in order to avoid the
direct r6ute across the desert and through the midst of the
Bedouins, the post-road makes a great circuit from Nisibis
by Jeziret ibu'Omar to Mosul. A second route crossed
the Eujil'-rates somewhat more to the south, and joined the
other via Harran and Rhessena. The principal crossing
of the earlier times (Xenophon) 'svas at Thapsacus, almost
opposite Kakka; and it will be remembered also how
important a part Thapsacus (Tiphsah) plays in the Old
Testament. Sometimes a route along the Euphrates to
Babylonia was followed, as is still frequently done by
caravans at the present day ; but even in ancient times
this cour.«e was attended by more or less difficulty, the
country being occupied by the chiefs of independent
Arab tribes, with whom the travellers had to come to
terms.
The ancient condition of things must consequently be
con.sidered as essentially analogous to that of the present
day ; the central districts away from the rivers were occu-
pied at certain seasons, according as they yielded pasture,
by nomadic cattle-grazing tribes, the physical character of
the country being then and now the same on the whole as
that of the SjTian desert, which belongs not to Syria
but properly t-o Arabia. On the banks of the rivers were
settled half-nomadic Arab tribes, — tribes, that is, which
were more or less on the way to the agricultural stage, or
which, having become altogether agricultural, had never-
theless, owing to frequent intercourse with the Bedouins,
lost little of their original character, and even maintained
their independence. The same movement takes place over
and over again ; Arab tribes migrating from Arabia, that
■ fficina gentium, gradually settle down wherever circum-
■^tances prove favourable, and by this very change in theii-
mode of life make their first step towards civilization. In
this way a continual stream of Arabs has flowed into
the civilized countries of Mesopotamia. On the Assyrian
monuments are figures of Arabs riding on camels ; evidently
the Assyrians had can'ied on war against the Bedouins
settled in their territory. At an early period the Tai Arabs
were the neighbours of the Aramaeans, and consequently all
Arabs bear in Syriac the name of Tay6y^. The district
between Jfosul and Nisibis received the name B^th ' ArbAyiS
from its-being occupied by Arabs. These Tai Arabs, whose
original home was Central Arabia, arc still settled partly
near Nisibis and partly east of Mosul ; but they have to
some extent lost their old noble^Bedouin manners. , The
wandering Arab tribe *^ which "'af the present* time is
dominant in Mesopotamia is the Shanimar ; they have
driven back the AJaeze, the most powerful, tribe of the
10—4
Syrian desert. It is only two or three generations ago
that the Shammar came from Nejd ; but they have ah-eady
broken up into two great parties. The head of the one
division is FerhAn, who has more or less completely sub-
' mitted to the Turks, and has consequently obt.iined the
title of pasha ; to him adhere the Shammar tribes between
I Mosul and Baghdad, and those al.so to the east of the Tigris.
! The head of the tribes who roam over the greater part of
Mesopotamia— pasturing their camels and sheep to the
east of the Chaboras in the colder season and to the north
in the hotter — is the chivalrous Filris. These western
I tribes are totally independent of the Turkish Government,
and have offered determined opposition to the attempts of
the authorities at D^r to force them to a settled way of
life; they still lay the peasants of Mesopotamia under
contribution by exacting Khuwwe, " brother-money," or a
portion of grain. The Shammar live in almost perpetual
feud with their relations to the east, and especially with the
Anezo on the Syrian bank of the Euphrates, the so-called
Shilmfye. Many other Bedouin tribes might, here bo
mentioned ; but it may be enough to name the Deldm on
the Euphrates as an example of a tribe just in process of
becoming agricultural. In the northern parts of Mesopo-
tamia there are a number of tribes of mingled Kurds and
Arabs which have to a greater or less degree abandoned
their tents for fixed habitations and the tillage of the
ground; such are the Beraziye near Orfa, the Milliye
between Orfa and Mardin, and the Kikfye nearer Mardin
and also in the neighbourhood of Mosul. It is extremely
hard to obtain trustworthy statistical information about
the number of the Bedouins ; the Shammar may have a
total strength of some 3500 tents. In the difficult contests
which it has to carry on with those independence-loving
tribes, the Turlcish Government acts in general on the
jjrinciple climde et imjyera.
The Kurdish element only appears sporadically in the
true Mesopotamian plain ; but the Yezidis, who form the
popidation of the Sinjar range, may be referred to this
stock. He who encounters the uncanny figure of one of
these people will hardly be able to restrain a slight shudder,
especially if he remembers the graphic descriptions of the
Yezidi robbers in Morier's Aj/esha. Of the old Aramjcau
peasantry there are no longer any important remains in the
plain, the Arama2ans having withdrawn farther into the
Kurdish highlands, where, in spite of their wild Kurdish
neighbours, they are more secure from exactions of every
kind. The plain of the northern country of the two rivers
was at one time richly cultivated, and owed its prosperity
to this industrious people, who formerly played so distin-
guished a part as a connecting link between the Persians
and the Roman empire and afterwards between the Western,
and the Arabian world, and whose highest culture was
developed in this very region. Quite otherwise is it now.
Ill the plain there are almost no remains of the common
Aramaean tongue. Apart from the scattered areas in which
Kurdish prevails, the ordinary language is a vulgar Arabic
dialect ; but both Kurdish and Aramjean (Syriac) have
exercised an influence on the speech of the Arab peasant.
Finally it must be mentioned that certain Turcoman hordesi
roam about the Mesopotamian territory.
In climnte and in the character of its soil, as well as in its ethno-
graphic history, Mesopotamia holds an intermediate position. - In
this aspect also we must maintain the division into two quite distinct
zones. Tlie southern half consists mainly of grey, dreary, flats
covered with selenite ; and ffvpsum everywhere makes its apnearanco
a little below the surface ; bitumen is not unfrequent, and ne»e and
there it rises in petroleum wells. In the .solid strata of gypsum aud
marl the rivers have carved out valleys, from a quarter to half a mile
broad and from 40 to 50 or even 100 feet deep, wliich with their arable
soil contrast with the barren surface o£ the more elevated desert
(chol). Especially below Balis there are marl-hills capped witli
gvpsum. and alluvial plains (so-called Juiw'ts) of considerable exteut
XVI. — 7
50
MESOPOTAMIA
have been formed. '. The bauks of the rivers are there lined with a
luxuriant growth of tamarisks. Occasional swamps and small
lagoons occur ; and the marl shows a more or less marked efflores-
cence of salt. In tin's part of the country fro»t is rare even in
winter ; in siimmer the heat is of extraordinary intensity, and
during the whole season from ^[ay to the close of October it is but
slightly modifiL-d by the night-dews. During the sand storms
wliich frequently blow from the West Arabian desert, the tempera-
ture may rise to 50° C. (122° Fahr.),and this same excess of heat will
then prevail through seven degrees of latitude in the whole valley of
the Euphrates and Tigris from the Persian Gulf to the foot of the
mountains. For, considering the strong radiation which takes
place over what is now the uniform surface of the Mesopotamian
soil witli its almost complete absence of evaporation, there is
nothing to hinder this warm zone extending in summer to the
upper half of the country. In winter, on the other hand, this latter
region has quite a diflferent climate. From the mild coasts of the
Mediterranean the cold increases from west to east. In the spurs
of the Taurus, consequently, the winter cold extends far to the south,
and the influence of the snow-covered ridgos spreads far into the.
Mesopotamian ]>lain. Snow and ice are thus not unfrequent in the
higher part of the plain, and the temperature may fall as low as
-10° C. (14" Fahr.), especially if the cold north winds are blowing.
That inland region too is cut off from the influence of the mild air
of the Muditerranean by the coast ranges. For this reason the
vegetation is of a less southern character than that of the Mediter-
ranean countries in tlie same latitude. In tlie spring the green is
soon parched out of existence. In this way the northern district
of Mesopotamia combines strong contrasts, and is a connecting link
between the mountain region of western Asia and the desert of
Arabia. On the other hand the country to the south of Mesopotamia,
or 'Irak, has a warm climate, and towards the Persian Gulf indeed
the heat reaches the greatest extremes.
In Upper Mesopotamia, strictly so called, agi-iculture has sutVered
an extraordinary decline; in spite of excellent soil, very little of the
land is turned to account. In the western district the fertile red-
brown humus of the Orfa plain, derived from the lime of Nimrud
Dagh, extends to about 12 miles south of Harran.^ With a greater
rainfall, and an artificial distribution of the water such as existed
in olden times, agriculture would flourish. If spring rains are only
moderately abundant, wheat and barley grow to a great height,
and yield from thirty to forty fold. Rice is also grown in the richly
watered hill-encircled district of Seriij and on the. banks of the
Khabur. Next, millet and sesamum are the chief crops, — the
latter being grown for the sake of its oil, as the olive does not
succeed in this region. The abundance of wheat may be ^.itiniated
from the fact that during Layard's residence in ftlosul a camel-load
of 480 lb was worth four shillings, Durra {Holais Sorghum and
H. hlcolor), lentils, pease, beans, and vetches are also grown, as well
as cotton, safBower, hemp, and tobacco. Medicago sativa furnishes
fodder for horses. Among the fruits the most noteworthy are the
cucumbers, melons, and water-melons planted in great abundance
on the banks of the smaller streams. The figs of the Sinjar
mountains are celebrated for their exceptional sweetness. Timber
trees are few ; plane frees and white poplars are planted along
the streams, auvl a kind of willow and a sumach flourish on the
banks of the Euphrates. The palm-trees which appear on the
banks of both the rivers farther south do not come so far north.
On account of the hot diy summer the orange does not succeed.
Of the great forest which existed (?) near Nisibis in the time of
Trajan no trace remains ; but the slopes both of the Masius
mountains and of the Jebel 'Abd-el 'Aziz, as well as, more especi-
ally, those of the Sinjar range, are still covered with wood.
i The wide treeless tracts of the low country of Mesopotamia are
covered with the same steppe vegetation which prevails from Central*
Asia to Algeria, but there is an absence of a great many of the
arborescent plants that grow in the rockier and more irregular
plateaus of western Asia and especially of Persia. This comparative
poverty and monotony of the flora is partly due to the surface being
mainly composed of detritus, and parily to the cultivation of the
country in remote antiquity having ousted the original vegetation
and left behind it what is really only fallow ground untouched for
thousands of years. Endless masses of tall weeds, belonging to a few
species, cover the faceof the country,— large Cruciferse, Cynarem, and
Vmbdlifcrm disputin^j the possession of the soil in company with
extraordinary quantities of liquorice {Qly^cyrrhiza glabra and
echlnata) as well as Layon.ychinvi'a.Jid the white ears of the Impcrata.
lu autumn the withered weeds are torn up by the wind and driven
immense distances. Among the aromatic plants, which even
Xenophon mentions in Mesopotamia, the first place belongs to the
species of wormwood {Artemisia), which cover wide areas, and the
second to LabicUx, such as species of thyme and Salvia, which, how-
ever, become rarer in the low country. With few exceptions there
arc none but cultivated trees, and these are confined to tlie irrigated
districts on the Euphiates and the Shatt ; a few willows, a Pi/rtm,
tamarisks, a Rhus, a Rubies, on the banks of the rivers, and the
wiUow-like Popuhts cxq)hraiica, which grows from Dzungaria to
Morocco, make up the list of the infSgenons kinds. In the wide
belt of swamp which lines the Shatt el-' Arab in the low country of
'Irak 'Arabi there are boundless reaches of gigantic sedge inhabited
by a rich fauna, especially of birds such as pelicans and flan«ngocs.
From the south, or in other words from tne tnie desert and oasis
country of Arabia, the date-palm spreads up the valley to some
little distance above Baghdad; and especially along the Shatt it
yields rich crops of fruit, which are exported to India. With the
exception of a tew truffles, capers, liquorice, and such like, there are
few wild food-plants. The cycle of vegetation begins in November.
The firstwinter rains clothe the plain with verdure, and by the
beginning of the year a number of bulbous plants are in bloom —
Aiiiaryllidm, Liliacex, SLXidColchicuvi, The full summer develop-
ment is reached in June ; and by the end of August everything is
burnt up.
The lion is said to roam as far as the Khabur; but in any case it
is at least much less frequent than in the time of the Ass3'rian8,
when the lion-hunt was a recognized form of spori. The wild ass
too is very rare ; but on the other hand wild swine, hyaenas, jackals,
cheetahs, and foxes are extremely abundant. Wolves are said to
exist in the plain, and among others a variety of black wolf {Canis
hjcaon). Particularly numerous in the steppe are th6 antelope
species ; and herds of gazelles are frequently met with. Beavere are
said to have been observed on the Euphrates. Jerboas, moles, por-
cupines, and especially the common European rat, abound in the
desert ; bats are numerous ; and the long-haired desert hare is also
found. Among the domestic animals in tuis steppe country the
camel holds the first place ; and next come goats and sheep ; but the
Bedouin sheep is not the ordinary fat-tailed variety. The common
buffalo is often kept by the Arabs and Turcomans on the Euphrates
and the Tigris ; and on the Euphrates we also find the Indian zebu,
which is still more frequent in the districts farther to the south.
Bird-life is very rare in tlte southern parts ol.^the plain ; though
on the Euphrates there are vultures, owls, ravens; &c., as well .i.'i
falcons {"i Tinnunculus alaudarius) which are trained to hunt.
Among game-birds are some kinds of doves, francolins, part-
ridges, wild ducks and geese, and in the steppe bustards. The
ostrich seems almost to have disappeared. Largo tortoises are
numerous.
In conclusion it is necessary in supplement to t"he article Irak
to say something of the district of Babylonia, often (though wrongly)
included under the name Mesopotamia. Here we have to do with
a fundamentally different region, for it consists in the main of
alluvial formations, a few scattered reaches of sand only now and
then appearing in the level depression not tilled up by the alluvium.
The mass of solid matter which the rivers bring down and deposit
is very considerable ; it has been ascertained that the maximum
proportion for the Euphrates in the month of Januarv is -gVi ^^d
at other times ^-j ; lor the Tigris the maximum is y^. As
regards the physical character of the allu\ia, in the most northerly
portion the soil is pebbly, the pebbles consisting almost solely of
variously coloured flints and occasional small fragments of gypsum.
This is succeeded by a continuous formation of clayey soil, in part
argillaceous and argillo-calcareous, but covered with mould and
sand, or the more tenacious clay of frequent inundations.
In general, the northern plains of the interior have a slight
but well-deQued southerly inclination with local depressions. The
territory undulates in the central districts, and then sinks away into
mere marshes and lakes. The clay, of a deep blue colour, abounds
with marine shells, and shows a strong efflorescence of natron and
sea-salt, the latter derived from the decomposition of vegetable
matter. When the aoil is parched up the appearance of tho
mirage (serab) is very common. As extensive inundations in
spring are caused by both the rivers, especially the Tigris, great
alterations must have taken place in this part of the country
in the course of thousands of years. It has been asserted that in
former times the alluvial area at the mouth of the river increased
one mile in the space of thirty years ; and from this it has been
assumed that about the 6th century B.C. the Persian Gulf must
have stretched from 45 to 55 miles farther inland than at present.
The actual rate of increase at the present time is about 72 feet per
annum. For this reason we cannot decide much iu regard to the
former physical configuration of southern Babylonia; but it is at least
certain that the Euphrates and the Tigris reached the sea as inde-
pendent rivers. Ritter estimates that in the time of Alexander the
Great the embouchures were still separated by a good day's journey ;
and, though they cannot now bo traced, great alterations have
probably taken place in the upper portions of the rivers as well as
in the country near the mouths. Assyriologists tell us that more
than thirty-five canals are known by name f>*om the Babylonian
period ; but it is extremely difficult, or rather it has proved hitherto
impossible, to identify them either with those actually existing or
with those mentioned in classical authors,, in the Babylonian
Talmud, or in Arabian writers. To the west of the Euphrates waa
to bo found the Pallacopas channel, and we still have the Hindiy*
channel in the same quarter. The country between the rivers more
particularly was traversed by such secondary branches. Begiuninjf
MESOPOTAMIA
ifrom the Euphrates we must mention the Saklamye cliannel (Nahr
'Is4), the Nahr Melik, the Nahr Zcmbeiani'yc, and c.™ciallj' the
Nahr-en-Nil, constructed by tlie famous Omayyau governor
Hajjdj. Ea»tv.arJs from the Tigris strikes the great Nahrawan
channel ; and riglit through the country of tlie tno rivers runs
the Shatt-el Hai from Kiit-el-'Amara, almost due south to the
Euphrates, parallel with the Shatt-el-Kclir. Many of these have
been silted up; from those, however, which are still maintained
there is derived a considerable revenue, and by the restoration
of many of the old channels, traces of which are met with at
every step, the country might be again raised to that condition
of higli civilization which it enjoyed not only in antiquity but
partly even in the time of the later caliphs. The classical writers
are unanimous in their admiration of this country ; and it is at
least certain that nowhere else in the whole world was the principle
of the application of canals to the exigencies of agriculture worked
out so successfully. The most luxuriant vegetation was diffused
over the whole country ; and three crops were obtainable in the
year. It is this alone which makes it intelligible how this region
in the most remote antiqnity attained a high civilization, and for
centuries played, it may be said, one of the principal parts in the
history of the world. In the matter of civilization, indeed, no
country of the ancient world was its equal ; a multitude of great
cities once flourished within its borders. Even the Arabic writers
are unanimous in regard to the extremely favourable influence
which the character of the country exercised on the intellectual
activity, spirit, and capacity of its inhabitants. Wo need not here
discuss the question recently started as to whether the Biblical
garden of Eden is to be sought in this locality, two canals of the
Euphrates and Tigris being identified with the Gihon and Pison of
Gen. ii.^ but it is certain at least that this lower country of the
two rivers might well pass in antiquity for the ne plus ultra of
civilization, and exercised the most powerful political and intel-
lectual influence on the surrounding regions. The question often
raised as to whether the Semites were derived from this district
may also be left untouched. From the Bible we know that an
ancient name of the district was Shinar, though this has not
hitherto been discovered in the cuneiform inscriptious. The name
Rush is applied in the Bible to its oldest non-Semitic inhabitants.
The northern half of the country was called Akkad, the southern
Sttiner. But it must not be forgotten that the rivers never formed
ethnographic and political boundaries ; and thus Sumer extended
to the coast of the Persian Gulf and Akkad as far as the Lower Zab,
the eastern afllucnt of the Tigris. As a less ancient designation
of the whole country may be reckoned mat Ktilda, the country of
the Chaldceans (Hebr., erels Kasdtm) ; originally Kalda is said to
have designated central Babylonia. Of still later date is the name
derived from the capital, the country of Babel {ercts Babel), as an
equivalent of which m4t BMtlH appears in the cuneiform inscriptions
(in the. Darius lists Babtrxi). From this was developed the Glreek
designation Babylonia, BaRuKuvia (as early as Xenophon). That the
country was densely peopled may be gathered from the fact that about
704 B.C. eighty-nine fortified towns and eight hundred and twenty
smaller places in the Chaldasan country were captured during one
military expedition. Of separate districts of the country we may
mention Karduniash, the district in the vicinity and especially to the
north of, Babylon ; and southward by the sea-coast the important
country of Bit Yakln, governed by kings of its own. At a later date
we find on the coast and at the moutli of the Pallacopas canal the
maritime town of Teredon, which is also mentioned by the classical
writers. Besides Babylon and Borsippa, the larger cities were the
double city of Sippar (Sefarvayim, 2 Kings xvii. 24, 31) and Akkad
on the left bank of the Euphrates on the present J^'ahr 'Isa ; Erech,
i.e., Warka, on the left bank of the Euphrates; Ur ou the Palla-
copas, not far from the place where the Shatt-el-Hai falls into the
Tigris ; Kippur, i.e.. Tell Niffer ; Kutha (2 Kings xvii. 24), Kahie
(Gen. X. 10), in the north, Opis at the junction of the Adhem
(Physcus) with the Tigris. Huge mounds give evidence of the
extent of these cities. A number of the canals were navi^^ble
and at the same time, when the bridges were destroyed," they
formed defensive moats against the incursion of enemies from the
north. And the same purpose was served by the great wall (after-
wards the Median Wall of the Greeks) which ran across the country
from river to river between the points of their nearest approach.
Duriug the period of Greek domination a Greek city, Seleucia,
which afterwards attained great prosperity, was founded by
Scleucus I. in on extremely favourable situation on the right bank
of the Tigris. In the south of the country, too, there was a Greek
seaport town first called Alexandria on the Tigris and afterwards
Antiochia. After the conquest of Babylonia by the Parthians
(130 B.C.) a small Arabian kingdom grew up in those parts called
Characene or Mesene, after the town of Chara; or Maisan. It was
under Parthian and for a time under Roman supremacy. The city
of Vologesia, founded by Vologeses to the south-west of Babvlon,
nea* Ullais, in the neighbourhood of the later Kufa, was one of the
capitals of the Parthian power. In the time of the Sasanids, too,
as well as in that of the Parthians, the country of the lower
51
Euphrates and Tigris played a leading part ; it formed in fact th-*
mam centre of the Persian kingdom. The city of Ctesiphon,
founded by the Greeks on the east side of the Tigris opposite
beleucia, was the w-jnler residence of the Parthian kings, and the
JITJ'""^ ."I"'*' »f. "'«, Sasanids. Under the name of Madain
(IJe Cities) It contuiued to flourish till the rise of Baghdad in the
9th century The neighbourhood of Ctesiphon was Called in the
tune of the Sasanids Sunstan, a translation of the Aramarau desi".
nation Betn-Aranaye, "country of the Syrians," for the land w°i
mainly rvMi.ied by Aramaans. By a notable substitution tl,-
Arabs aftenvarils gave the name Nabat, i.e., NabatiEan.s to the--
Aramsean peasantry, who, it may be added, were already found ■'!
these parts at the time of the Babylonian empire.
On tlie west side of the Tigris the Arab kingdom of Hi'ra formed
the bulwark of the Sasanid power. As the result mainly of the
battle of Kadisiya (east of Hira) in 635 A.D., the whole of this
wealthy country fell into the hands of the Moslems, and it soon con-
stituted the centre of their ijower, especially when the Abbasids
with true political insight, transferred thither the capital of the
empire and founded Baghdad. The chief cities of the older Arabi"
period were Kiifa (in the neighbourhood of the earlier Hira to the
south of ancient Babylon) and Basra (or Bi'S.sonAH, q v.) in the
neighbourhood of the earlier Maisan. After these two cities the
country was divided into the Sawad, "rich arable district" of
Basra and that of Kufa. Sawad was also employed as a name for
the whole country ; and more or less identical with this designa-
tion is the name 'Irak still in use. Sometimes also the term Sawad-
el- Irak is employed ; but at a later date the country is distinguished
as Irak Arabi (Arabian 'Irak) from the Persian 'Irak 'Ajemi to the
east, the ancient Jledia. The Arabian geographer Yakut makes the
distinction that the country called Sawad reaches farther to tha
north (viz., to the district of the Upper Zab).
Abulfeda gives the boundaries of Irak as follows:—" In the west
of the country lie El-Jezii-a and the desert, in the south the desert,
the Persian Gulf, and Khuzistan, in the east the mountain country
as far as Hohvan (near the principal pass through the Zagrus
range). Thence the boundary runs again towards Mesopotamia.
Thus the greatest breadth of 'Irak is in the north, and its narrow
extremity is formed by the island' 'Abbadan in the Shatt-el-' Arab
(the united Euphrates and Tigris) to the south of Basra?' From
what has been said it.appears that 'Irak extended far beyond the
country between Euphrates and Tigris. ' Abulfeda says clearly that
Irak lies on the Tigris as Egypt on the Nile ; for according to this
view the Tigris flows through the middle of the country. 'Irak
consequently lies between 30° and 34"' 30' N. lat. and between 44'
and 48° 30' E. long. ; of its area it is impossible to form an estimate
under such varying conditions. For some details see Baghdad.
From the union of the rivers upwards, in the case of the Euphrates
as far as 26° N. lat. (above Eakka), in that of the 'Tigris to 35° N.
lat, the valleys are known as ei-':6r, the depression, in opposition to
the more elevated desert-plateau. It has been surmised that in thjs
name is to be recognized the Diira of the Old Testament (Daniel
iii. 1).
Very little of the ancient condition of the country has been pre-
served ; and there are now but few remains of ancient buildings,
scarcity of stone having all along led to the use of bricks. 'Irak
has played its part. It is only by the expenditure of immense
sums, far beyond the financial capacity of the Turkish Govern-
ment, that the ancient canals could be restored and the swamps
formed by them drained. The whole land falls into two unequal
portions, — an extensive dry steppe with at any rate a healthy
desert climate, and an unhealthy region of swamps. There is a
good deal more agriculture along the Euphrates than along the
Tigris ; but swamps, with almost impenetrable reed tliickets, com-
posed of a kind oi Agrostis, are at the same time much more exten-
sive. The slightly more elevated districts are the special habitat
of the date palm, which by itself forms dense groves bordering the'
banks particularly on the lower Euphrates, for a distance of several
days' journey. This part of the country consequently has a some-
what monotonous but in its own way imposing aspect. A luxu-
riant vegetation of water-plants is to be found in the swamps,
which are the haunt of numerous wild beasts — wild swine, lions,
different kinds of aquatic animals and birds. The swamps aro
inhabited by a wild race of men, dark of hue, with many negroes
amongst them. They live in reed huts, and cultivate rice ; and
they weave straw mats. In the main they keep pretty free both of
the Turkish Government and of the semi-Bedouins and Bedouins of
'Irak. The Khazael especially who dwell to the south of ancient
Babylon often give the Government trouble, through their passion
for independence. Less turbulent are the Bedouins in the interior
of the country — the Zobeid, the Afaij, and the Abu Muhammed ; but
oil the other hand the Beni Lam (7500 tents strong), who occupy the
great tract of country east of the Tigris to the south of Baghdad,
have often been a source of great annoyance to the pashas of that
city. A still more difficult task is the management of the Sham-
mar, who come and pitch their tents to the south-east of Baghdad ;
and also the Muntefitch on the southern Euphrates put the whole ad-.
62
M E S — M E S
miiiistrative and diplomatic skill of the Turkish olTicialsto the test.
The Turkish influence has here made at one time great advance
and at another lost all the ground it' had gained, — the rich and
powerful sheikhs of the Muntcfilch soraetiiiies becoming for a season
rulers over the whole of Southern 'Irak and even over the town of
Basra. The present writer once visited tlic great sheikh Kasir in
his camp near Siik-csh-Shiyukh ; and he received the impression
of having to do with a very remarkable and astute personag,?,
I^The old Syrian population of 'Iiuk has almost entirely dis-
api^arcd ; the few remnants left are distinguished by a 'special
religion, in regard to which see the article Mand^eans. Etlmo-
p^phically the country is subject to a double iiiflueuce. Ou the
one hand the connexion with Nejd, the. central plateau of Arabia,
continues uninterrupted ; the emigration from that region being
mainly directed towards 'Irak and Jezira, Tn Baghdad even, the
'Agel-Bcdouins from Central Arabia have a quarter of their own.
(With the earnings obtained in these i-ich districts the emigrants
return to their homes. But quite as strong at least is the influ-
ence of Persia. Persian customs are in fashion ; in Baghdad
there is an important Pei"sian quarter ; and Kerbela and Jleshed
*Aii to the west of the Euphrates may be considered regular
Persian "encbves." In these places are buried the son-in-law of
Moliammed, the caliph Ali, and his son Hosein (in Kerbela), the
chief saints of the Shiite sect ; and their tombs are not only shrines
of pilgrimage to the living, but the dead are brought by countless
caravans from Persia to be buried in ground which they have made
holy. The neighbourhood of Kerbela reeks with the odour 'of
corpses ; aud from the midst of them pestilence has often begun its
march. Throughout the whole of 'Iiuic the Sbiites have mauy ad-
herents,— for example, the Khazael already mentioned. Persian
influence prevails on the Arab population of 'Irak, and the inter-
mingling of the races can still be very clearly traced ; in this dis-
tant corner of the Turkish empire a more international tone prevails
than in any other district. And, however sl.iall when compared
with former times the commercial and intellectual intercourse of
various nations in these regions may be at the present day, the
attentive observer must notice that such intercourse does still
exist, though within restricted limits. No trace, indeed, is to be
found of that rich intellectual development which was produced
in the time of the calijihs through the reciprocal action of Persian
and Arabic elements. Still the quickwitt^ness of the inhabitants
of 'Irak makes a decided impression on the traveller passing through
Asiatic Turkey ; and one might venture to prophesy that the
country might to some extent recover its former position in the
world, especially if English influence from India were more widely
extended, and should lead to the construction of a railway. The
trade which passes through 'Irak is even now not unimportant ;
horses, for example, are expoited in considerable numbers from
southern 'Imk to India. But it might be very much improved, as
the country, it is said, could support five hundred times as many
inhabitants as it actually contains. Thei-e is also a considerable
export of dates, a fruit which forros the chief sustenance of a great
number of the inhabitants ; and the breeding of cattle {especially
buffaloes) is extensively carried on. Only a few steamboats as yet ?
navigate the 'majestic nvers. Communication by water is carried J
on by means of the naost primitive craft. Goods are transported j
in the so-called " terrades," moderately big high-built vessels, i
which also venture out into the Persian Gulf as far as Kuwet.
Passengers are conveyed, especially on the Euphrates, in the
meshh^, a very long and narrow boat, mostly T)ushed along the
river bank with poles. The Mesopotamiau *'kelleks" — rafts laid
on goatskin bladders — come down as far as Baghdad, where round
boats made of plaited reeds jiitched with asphalt are in use. At
Basra, on the other hand, we see the "belem," boats of a large
size, having the appearance of being hollowed out of tree trunks,
and partly in fact so constructed. Throughout 'Irak in general
Indian influence is paitially at work ; in the hot summer months,
for instance, when the natives live in underground apartments
(serdab), the Indian punkah is used in the bouses of the rich. As
regards language, the local Arabic dialect has evidently been
affected on the one hand by Persian, on the other by the Bedouin
forms of speech.
Sec Rltl-pr. Dlf ErdiuntU von Alien, 2(t e<L vol. vli., 10th and 11th parts, Berlin,
1843. 1844 ; Cliesncy. Expedition/or the Survey o/the Riven Euphrates and Tigris,
2 vol3., London, 1850; W. Alnswurth, Researches in Assyria, Bahy/onia, and
Chatdxa, London, 1838 ; Fr. Delitzsch. Wo lag das Parodies t Leipsic, 1881. Map;
Kicpeit, Die Eupkr'at- und Tigrisldnder, Berlin, 1854. (A. SO.)
MESSfiNE, the chief city of Messenia, founded, under
the auspices of Epaminondas, as a bulwark against the
Spartans. After the battle of Leuctra that general sent
to all the exiled Messonians, — in Africa, Sicily, or Italy, -^
and invited tliem to return to the land of their fathers.
Many came with eagerness, and in 369 B.C. the city was
built by the combined army of Thebans under Epaminondas
and Afgives under Epiteles, assisted bv the Messeiiians
themselves. The site was chosen in conformity with a
vision which appeared to Epaminondas, and the walls
were raised to the sound of flutes playing the airs of
Sacadas and Pronomus. The citadel was erected on
the summit of Mount Ithome, and the city on its southern
slope and in the adjoining valley. City and citadel were
enclosed by a wall 47 stadia in length. Near the centre
of tlie city was the agora, with a famous spring called
Arsinoe, and various temples and statues, among the latter
an iron statue of Ejiaminondas. The Hierothysion con-
tained many statues of gods and heroes, among them a
bronze statue of Epaminonda.s. In the gymnasium were
statues of Hermes, Hercules, and Theseus by Egyjjtian
artists. In the stadium was a bronze statue of the great
hero ■ Aristomenes, who had a sepulchral monument else-
where in the city. On the summit of the citadel was a
famous spring called Clepsydra, and near it a temple of
Zeus Ithomatas, with a statue by the famous Argive artist
Ageladas, executed originally for the Jlcssenian Helots
who settled in Naupactus (see Messenia). It was in
honour of this statue that the festival of the Ithomaea was
performed.
The situation of Messene is one of the finest and most
romantic in the world. The view of Mount Ithome, with
its level summit and its ancient and mediajval ruins, as
one issues from the Langadha Pass in the Taygetus
mountains, is beautiful beyond description. And the
view from the summit of the mountain itself, which rises,
steep and rugged, to the height of 2631 feet, and is
crov.Tied by the ruins of fortifications of Cydoiaean work-
manship, is enchanting, hardly equalled by any other in
Greece. Near the middle of the ruins of the lower city
stands a wretched vUlage named JIavrommati (Black Eye),
so called from the Turkish name of the spring Arsinoe,
which still flows as plentifully as in the old day.s. These
ruins are the most imposing in Greece, and furnish the
finest existing specimen of Hellenic military architecture.
Almost the entire circuit of the ancient walls can be traced,
and in some places they are standing to their full height.
They are built of large hewn stones laid in beautifully
regular layers without mortar, and are surmounted by
tower.5, of which there seem to have been originally over
thirty. Seven of these are still in a good state of preser-
vation, and bear testimony to the thoroughness of the great
eiiteriirise undertaken by Epaminondas. Two gates can
still be distinguished, one on the slope of Mount Ithome,
the other (the northern or Megalopolis gate) on the north
side. The Litter is a dipylon or double gate, opening into
a circular enclosure 62 feet in diameter. The walls of
this enclosure are built with extreme care, and the soffit
stone of the inner portal, which has .been partly moved
from its place, reminds one of the lintel of the so-called
treasury of Atreus at Mycenae. It is 18 ft. 8 in. x -t f t. 2
in. X 2 ft. 10 in. Within the town several ancient sites
can still be distingtiished — the stadium, the theatre, and
several temples.
MESSENIA (in Homer Messene), a state of Greece, and
the most westerly of the, three peninsulas of the Pelopon-
nesus. Its area is a httle over 1160 square miles. It is
separated from Elis and Arcadia on the north by the river
Neda and the Nomian mountains, and from Laconia on the
east by the lofty range of Taygetus. The other sides are
washed by the sea, which indents its shores with four gulfs
or bays, — Messenia, Phwnicus, Pj'lus, and Cyqiarissus. On
its south-w.est corner are the (Enussa; Islands, and ojipo-
site the bay of Pylus (Navarino) the famous Sphacteria.
The interior is divided by mountain chains into fertile
[ilains, watered by rivers, the chief of which is the Pamistis
(with its tributaries Leucasia, Charadrus, Amphitu.s, and
Alia), falling into the Messenian Gulf. The great valley
M E S — M E S
63
of this river is di\ided, near Mount Ithome, into two
distinct parts, the plain or basin of Stenyclarus on the
north, and the plain of ^facaria, so called from its extreme
fertility, on the south. The climate is delightful.
The earliest inhabitants of Messenia were Leieges, whose
capital was at Andania. After these came ^tolians, whose
chief centre was at Pylus. After the Dorian conquest the
country was divided by Cresphontes into five parts, whose
chief cities were respectively Stenyclarus, Pylus, Khion,
Hyamia, and Mesola. The towns of Messenia were not
numerous. Homer mentions Pylus (the seat of the
Thessalian Neleids), Amphigeneia (possibly the same as
Ampheia), Dorion, jEpeia (possibly Methone), CEchalia,
Pharse, Antheia (probably the later Thuria), Pedasus, and
Ira (the later Abia). Other important towns were Asine,
Corone, . Limna;, Carnasium, Cyparissia, and, finally,
Mcssene.
Of the history of Jfesseiiia before tlie Dorian invasion little is
known except a few fables related by Pausanias. Two generations
after the Trojan war, tlie country w.13 iuvadeil by the Dorians, who
expelled the Neleids and conferred the sovereignty upon Crespliontes,
■who seems to have been a po|>ular king. I'erbans for this reason
he was put to death by tbe chiefs along with aU his sous except
./Epytus. .Spytus was restored to the tliroue by the Arcadians,
took vengeance for his father's death, and became vei7 popular.
His line lasted througb several generations. We know little, of tlie
subsequent liistory of Messenia until the date of the Messcnian ware,
waged against Sparta. The ostensible and immediate causes of these
wars are variously assigned ; but the true cause was the cupidity of
Sparta. Our chief tnistworthy authority for the history of them
is the old elegiac poet Tyrteus ; but so little is known about them
that it is a matter of doubt in which of tliem the great hero
Aristomenes won his fame. The date of the first was from 743 to
724, of the second from 685 to 668 or, according to others, from
643 to 631 B.C Ithome was the centre of action in the first, Eira
in the second. The result of these ware was the complete subjuga-
tion of Jlessenia to Sparta. Its territory was parcelled out among
Spartans, and its towns handed over to I'ericcci and Helots. Many
of the inbabitants took refuge in Arcadia, but still more in Italy
and Sicily. A very large number settled in Rhcgium, whose chiefs
for many generations were of Messenian stock. About 200,000
remainetl behind in bondage. After the second war a large number
of Messenians settled on the Sicilian coast at Zancle, to wliich they
subsequently gave the name Messana (see Messina). In 464 B.c.
the Jlessenian Helots, taking advantage of an earthquake at Snarta,
revolted, and, though they were finally compelled to surrender in
455, they did so only on condition of being allowed to retire to
Xaupactus on the Corinthian Gulf. This city had been ofiered them
as a residence by the Athenians, ever glad to favour the foes of
Sparta.' Here the Jlessenians remaine<l for sixty years, luttil the
loss of the battle of /Egosjiotami deprivetl them of the protection of
the Athenians. They were then driven out, and had to find homes
in Cciihallenui and Zacynthus, or among their kinsmen in Rhemuni
and Messana. Some even went to Africa, and took U)i tlieir aboile
at Eues]ierid."e or Hesneridre, afterwards called Berenice. Things
remained in this condition until 369 B.C., when Epaminoudas,
having broken the j>ower of Sj^rta, rent from her Messenia, and,
collecting from all quarters the <\esceudants of the exiled iuliabit-
ants, helped them to found the city of Ml.<slxe (^.r.). Sparta
never gave up her claim to ilessenia, and made many attempts to
reconquer it, but without success. The ilesseuians maintained
their uul(?J>cndence until \46 B.C., when, with the Achaaus, they
were reduced under tlie power of Rome. From that time they fall
into the backgiouud of history. In the Middle Ages the country,
like the rest of the reloponnesus, was largely overrun by Slavic
tribes, as is shown by the numerous Slavic local names occuning in
it. At the establishment of Greece as a kingdom, Messenia was
constituted iifto a jtrovincc, with a governor or nomarch residing at
Kalamata {officially Kalamai), the nncieiit Phara'. The country,
though beautiful a'nd fertile, is still in a .Icplorably backward con-
dition, and the jioiniLitinn ii sjiarse and semi-barbarous. Agricul-
ture languishes, and the roads and bridges arc few and bad. More
deeds of violence occur in Mesjsenia than in any other jtart of Gn-cco.
With the excejilion of Kalamata, it contains no town of inii.ortani-e.
Xavarino. on the Gulf of Pylus, was the scene of the destruction of
the Turkish fiect inlS27.
MESSIAH (Dan. x. 2.=;, 15),'^ Mes.<!Ias (.lohn i. 41 ;
iv. 2.")), are. transcriptions (the first form modified by
refereiKe to the etymology) of tlie Greek Mecro-t'as
, (Mco-i'as, Mfffcio;), which in turn reitresents the Aramaic
■ >tn'L"0_()«iV(<n((), answering to the Hebrew ri'ran "the
anointed."' The Hebrew word with the article prefixed
occurs in the Old Testament only in the phrase ''the
anointed priest" (Lev. iv. 3, 5, 16; vi. 22 [15]), but
" Jehovah's anointed " is a common title of the king of
Israel, applied in the historical books to Saul and David, ■
in Lam. iv. 20 to Zedekiah, and in Isa. xlv. 1 extended
to Cyrus. In the Psalms corresponding phrases (My, Thy,
His anointed) ^ occur nine times, to which may be added
the lyrical passages 1 Sam. ii. 10, Hab. iii. 13. In the
intention of the writers of these hymns there can generally
be no doubt that it refers to the king then on the throne,
or, in hymns"* of more general and timeless character, to
the Davidic king as such (without personal reference to
one king) ; ' but in the Psalms the ideal aspect of the
kingship, its religious importance as the expression and
organ of Jehovah's sovereignty, is prominent. When the
Psalter became a liturgical book the historical kingship
had gone by, and the idea alone remained, no longer as the
interpretation of a present political fact, but as part of
Israel's religious inheritance. It was impossible, however,
to think that a true idea had become obsolete merely,
because it found no expression on earth for the time being ;
Israel looked again for an anointed king to whom the
words of the sacred hymns should apply with a force never
realized in the imperfect kingship of the past. Thus the
psalms, especially such psalms as the second, were neces-
sarily viewed as prophetic; and meantime, in accordance
with the common Hebrew representation of ideal things as
existing in heaven, the true king remains hidden with God.
The steps by which this resiJt >va3 reached must, however,
be considered in detaiL
The hope of the advent of an ideal king was only one
feature of that larger hope of the salvation of Israel from all
evils, the realization of )>erfect reconciliation with Jehovah,
and the felicity of the righteous in Him, in a new order of
things free from the assaults of hostile nations and the
troubling of the wicked within the Hebrew community,
which was constantly held forth by all the prophets, from
the time when the great seers of the 8th century B c. first
proclaimed that the true conception of Jehovah's relation
to His people was altogether different from what was
realized, or even aimed at, by the recognized civil and
religious leaders of the two Hebrew kingdoms, and that it
could become a practical reality only through a great
deliverance following a sifting judgment of the most
terrible kind. The idea of a judgment so severe as to
render jrassible an entire breach with the guilty past, arid
of a subsequent complete realization of Jehovah's kingship
in a regenerate nation, is common to all the prophets, but
is expressed in a gr«at variety of forms and images, con-
ditioned by the present situation and needs of Israel at the
time when each prophet spoke. As a rule the prophets
directly connect the final restoration with the removal of
the sins of their own age, and ivith the accomplishment of
such a work of judgment as lies within their own horizon;
to Isaiah the last troubles are those of Assyrian invasion,
to Jeremiah the restoration follows on the exile t3 Babylon ;
Daniel connects the future glory with the overthrow fcf the
Greek monarchy. The details of the i>rophetic pictures
aliow a corresponding variation; but all agree in giving the
central place to the realization of a real effective kingship
of Jehovah ; in fact the conception of the religious subject
' Tlie tiaiiscriptioii i< as ill Ttaaoip, Tfatrlp forllf ?, Onomastica,
cd. La;., y\\ 247. 2S1, Bcur. $ ii. 3. For the •termiuatiou as for
Sri, seeLafaide, Psill. Mr,iii>li., p. vil.
' The plural is found in Ps.alm cv. 15, of the patriarchs as conse-
Liated pei-son-t. , - .
» In Ps. Ixxxiv. 9 [10] it is disputed whether the anointed one w
■.he king, the priest, or the nation as a wliole.HS.Tlie secoud view la
perhaps lije best. -
64
MESSIAH
as the nation of Israel, with a national organization under
Jehovah as king, is common to the whole Old Testament,
and forms the bond that connects prophecy proper with
the so-called Messianic psalms and similar passages which
theologians call typical, i.e., with such passages as speak
of the religious relations of the Hebrew commonwealth,
the religious meaning of national institutions, and so
necessarily contain ideal elements reaching beyond the
empirical present. All such passages are frequently called
Messianic ; but the term is more properly reserved as
the specific designation of one particular branch of the
Hebrew hope of salvation, which, becoming prominent in
post-canonical Judaism, used the name of the Messiah as
a technical term (which it never is in the Old Testament),
and exercised a great influence on New Testament thought,
— the term " the Christ " (6 xpL(n6<;) being itself nothing
more than the translation of " the Messiah."
In the period of the Hebrew monarchy the thought that
Jehovah is the divine king of Israel was associated with the
conception that the human king reigns by right only if he
reigns by commission or " unction " from Him. Such was
the theory of the kingship in Ephraim as well as in Judah
(Deut. xxxiii. ; 2 Kings ix. 6), till in the decadence of the
northern state Amos(ix. 11) foretold the redintegration of
the Davidic kingdom, and Hosea (iii. 5 ; viii. 4) expressly
associated a similar prediction with the condemnation of the
kingship of Ephraim as illegitimate. So the great Judaean
prophets of the 8fh century connect the lalvation of, Israel
with the rise of a Davidic king, full of Jehovah's Spirit, in
whom all the energies of Jehovah's transcendental kingship
are as it were incarnate (Isa. ix. 6 sq. ; xi. 1 sq. ; Micah v.).
This conception, however, is not one of the constant
elements of prophecy ; indeed the later prophecies of Isaiah
take a different shape, looking for the decisive interposition,
of Jehovah in the crisis of history without the instru-
mentality of a kingly deliverer. Jerehiiah again speaks
of the future David or righteous sprout of David's stem
(xxiii. 5 sq. ; xxx. 9) ; and Ezekiel uses similar language
(xxsiv., xxxvii.) ; but that such passages do not necessarily
mean more than that the Davidic dynasty eiaU be con-
tinued in the time of restoration under a series of worthy
princes seems clear from the way in which Ezekiel speaks
of the prince in chaps, xlv., xlri. As yet we have no fixed
doctrine of a personal Messiah, but only material from
which such a doctrine might by and by be drawn. The
religious view of the kingship is still essentially the same
as in 2 Sam. vii., where the endless duration of the Davidic
dynasty is set forth as part of Jehovah's plan of grace to
His nation.
There are other parts of the Old Testament — notably
1 Sam. viii., xii. — in which the very existence of a human
kingship is represented as a dei)arture from the ideal of a
perfect theocracy. And so, in and after the exile, when
the monarchy had come to an end, we find pictures of the
latter days in which its restoration has no place. Such is
the great prophecy of Isa. xl.-Lxvi., in which Cyrus is the
anointed of Jehovah, and the grace promised to David is
transferred to ideal Israel (" the servant of Jehovah ") as a
whole (Isa. Iv. 3). So too there is no allusion to a human
kingship in J oel or in Malachi ; the old forms of the
Hebiew state were broken, and religious hopes expressed
themselves in other shapes.' In the book of Daniel it is
collective Israel that appears under the symbol of a " son
of man," and receives the kingdom (vii. 13, 18, 22, 27).
Meantime, however, the decay ami ultimate silence of the
living urophetic word concurred with the prolonged
political servitude of the nation to produce a most
^ The hopes which Hoggai and Zechariah connect with the nime of
Zjrabbahel, a descendant of David, hardly form an exception to this
statement.
important change in the tyjie of the Hebrew religion.
The prophets had never sought to add to the religious
unity of their teaching unity in the pictorial form in
which from time to time they depicted the final judgment
and future glory. Fgr this there was a religious reason.
To them the kingship of Jehovah was not a mere ideal,
but an actual reality. Its full manifestation indeed, to the
eye of sense and to the unbelieving world, lay in the
future ; but true faith found a present stay in the
sovereignty of Jehovah, daily exhibited in providence and
interpreted to each generation by the voice of the prophets.
And, while Jehovah's kingship was a living and present fact,
it refused to be formulated in fixed invariable shape. But
when the prophets ceased and their place was taken by the
scribes, the interpreters of the written word, when at the
same time the yoke of foreign oppressors rested continually
on the laud, Israel no longer felt itself a hving nation, and
Jehovah's kingship, which presupposed a living nation,
found not even the most inadequate expression in daily
political life. Jehovah was still the lawgiver of Israel, but
His law was written in a book, and He was not present to
administer it. He was still the hope of Israel, but the
hope was all dissevered from the present ; it too was to be
read in books, and these were interpreted of a future
which was no longer, as it had been to the prophets,
the ideal development of forces already at work in Israel,
but wholly new and supernatural. The present was a
blank, in which religious duty was summed up in patient
obedience to the law and penitent submission to the Divine
chastisements ; the living realities of divine grace were
but memories of the past, or visions of " the world to
come." The scribes, who in this period took the place of
the prophets as the leaders of religious thought, were
mainly busied with the law ; but no religion can subsist on
mere law ; and the .systematization of the prophetic hopes,
and of those more ideal parts of the other sacred literature
which, because ideal and dissevered from the present, were
now set on one line ■n'ith the prophecies, went on side by
side with the systematization of the law, by means of a
harmonistic exegesis, which sought to gather up every
prophetic image in one grand panorama of the issues of
Israel's and the world's history. The beginnings of this
process can probably be traced vrithin the canon itself, in
the book of Joel and the last chapters of Zechariah ; '■^ and,
if this be so, we see from Zech. tx. that the picture of the
ideal king early claimed a place in such constructions.
The full development of the method belongs, however, to
the post-canonical literature, and was naturally much less
regular and rapid than the growth of the legal traditions
of the scribes. The attempt to form a schematic escha-
tology left so much room for the play of individual fancy
that its results could not quickly take fixed dogmatic
shape ; and it did not appeal to all minds alike or equally
at all times. It was in crises of national anguish that .men
turned most eagerly to the prophecies, and sought to con-
strue their teachings as a promise of speedy deliverance in
such elaborate schemes of the incoming of the future glory
as fill the Apocai-yptic Liteeatuke {q.v.). But these
books, however influential, had no public authority, and
when the yoke of oppression was lightened but a little
their enthusiasm lost much of its contagious power. It is
not. therefore safe to measure the gencVal growth of
eschatological doctrine by the apocalyptic books, of which
Daniel alone attained a canonical position. In the
ApocryjJia eschatology has a very small place ; but there
is enough to show that the hope of Israel was never
forgotten, and that the imagery of the prophets had
' Seo Joel, vol. xiii. p. 706, and Stade's .irticlea "Deuterozacharja,''
Z.f. .1 TlMe Il'iss., 18S1-S2. Compare D;ir_. is. 2 for tho wsc of tho
older prophecies in llie solution of new problems of fal.!;.
M ii: S iS 1 A H
5;")
moulded that hope into certain fixed forms which were
taken with a literalness not contemplated by the prophets
themselves. It was, however, only very gradually that
the figure and name of the Messiah acquired the pro-
minence which they have in later Jewish doctrine of the
last things and in the official exegesis of the Targums. In
the very developed eschatolog)' of Daniel they are, as we
have seen, altogether wanting, and in the Apocrypha, both
before and after the Maccabee revival, the everlasting
throne of David's house is a mere historical reminiscence
(Sirach xlvii. 11 ; 1 Mac. ii. 57). So long as the wars of
independence worthily occupied the energies of the Pales-
tinian Jews, and the Hasmonsean sovereignty promised a
measure of independence and felicity under the law, in
which the people were ready to acquiesce, at least, till the
rise of a new jjrophet (1 Mac. xiv. 41), the hope that con-
nected itself with the house of David was not likely to rise
to fresh life, especiaUy as a considerable proportion of the
not very numerous passages of Scripture which speak
of the ideal king might with a little straining be applied
to the rising star of the new djTiasty (comp. the language
of 1 Mac. xiv. 4—15). It is only in Alexandria, where
the Jews were still subject to the yoke of the Gtentile,
that at this time (c. 140 B.C.) v.-e find the oldest Sibylline
verses (iii. 652 sq.) proclaiming the approach of the
righteous king whom God shall raise up from the East
(Isa. xli. 2) to establish peace on earth and inaugurate the
sovereignty of the prophets in a regenerate world. The
name Messiah is still lacking, and the central point of the
prophecy is not the reign of the deliverer but the subjec-
tion of all nations to the law and the temple.^
With the growing weakness and corruption of the
Hasmonaean princes, and the alienation of a large part of
the nation from their cause, the hope of a better kingship
begins to appear in Jud<ea also ; at first darkly shadowed
forth in the Book of £uoch (chap, xc), where the white
steer, the future leader of God's herd after the deliverance
from the heathen, stands in a certain contrast to the in-
adequate sovereignty of the actual dynasty (the horned
lambs) ; and then much more clearly, and for the first time
with use of the name Messiah, in the Psalter of Solomon,
the chief document of the protest of Pharisaism against its
enemies the later Hasmonceans. The struggle between the
Pharisees and Sadducees, between the party of the scribes
and the party of the Hasmonsean aristocracy, has been
described in Israel (vol. xiii. p. 423 sq.). It was a
struggle for mastery between a secularized hierarchy on
the one hand, to whom the theocracy was only a name, and
whose whole interests were those of their own selfish politics,
and on the other hand a party to which God and the law
were all in all, and whose influence depended on the main-
tenance of the doctrine that the exact fulfilling of the law
according to the precepts of the scribes was the absorbing
vocation of Israel This doctrine had grown up in the
political nullity of Judsea rnder Persian and Grecian rule,
and no government that possessed or aimed at political
independence could possibly show constant deference to
the punctilios of the schoolmen. The Pharisees themselves
could not but see that their principles were politically
impotent ; the most scrupulous observance of the Sabbath,
for example — and this was the culminating point of legality
^ould not thrust back the arms of the heathen. Thus
the party of the scribes, when they came into conflict
with an active political power, which at the same time
claimed to represent the theocratic interests of Israel, were
compelled to lay fresh stress on the doctrine that the true
deliverance of Israel must come from God and not from
mifa. We have seen indeed that the legalism which accepted
' I: SP-i'll., iii. 775, i/i)6ii laust unJoaMedly be read for vl6v.
Jehovah as legislator, while admitting that his executive
sovereignty asjudge and captain of Israel was for the time
dormant, would from the first have been a self-destructive
position without the complementary hope of a future
vindication of divine justice and mercy, when the God of
Israel should return to reign over his people for eve/.
Before the Maccabee revival the spirit of nationality was
so dead that this hope ky in the background ; the ethical
and devotional aspects of religion under the law held the
first place, and the monotony of poUtical serv-I'ude gave little
occasion for the observation that a true national life
requires a personal leader as well as a wTitten law. But
now the Jews were a nation once more, and national ideas
came to the front. In the Hasmonaean sovereignty these
ideas took a political form, and the result was the secular-
ization of the kingdom of God for the sake of a harsh and
rapacious aristocrac}'. The nation threw itself on the side
of the Pharisees; but it did so in no mere spirit of
punctilious legalism, but with the ardour of a national
enthusiasm deceived in its dearest hopes, and turning for
help from the delusive kingship of the Hasmona^ans to
the true kingship of Jehovah, and to His vicegerent the
king of David's house. It is in this connexion that the
doctrine and name of the Messiah appear in the Psalter
of Solomon. The eternal kingship of the house of David,
so long forgotten, is seized on as the proof that the
Hasmonaeans have no divine right.
*'Thou, Lord, art our king for ever .ind ever. . . . Thou didst
choose David as king over Israel, and swarest unto him concerning
his seed for ever that his kinship should never fail before Thee.
And for our sins sinnei*s (the Hasmonaeans) have risen up over us,
tiiking with force the kingdom whiih Thou didst not promiso to
them, profaning the throne of David in their pride. But Thou, 0
Loi-d, will cast them down and root out their seed from the land,
when a man not of onr race (Pompey) rises up against them. . . .
Behold, 0 Lord, and raise up their king the Son of David at the time
that Thou liast appointed, to reign over Israel Thy servant; and gird
him with strengtli to crush unjust rulers ; to cleanse Jerusalem
from the heathen that tread it under foot, to cast out sinners from
Thy inheritance; to break the pride of sinners and all their strength
as potter's vessels with a rod of iron (Ps. il 9); to destroy the law-
less nations with the word of his mouth (Isa. xi. 4) ; to gather a
holy nation and lead them in righteovsness. . . . He shall divide
them by tribes in the land, and nostranger and foreigner shall dwell
with them; he shall judge the nations in wisdom and righteousness.
The heathen nations shall scr^'e under liis yoke ; he shall glorify
the Lord before all the earth, and cleanse Jerusalem in holiness as in
the beginning. From the ends of the earth all nations shall come
to see his glory and bring the weary sons of Zion as gifts (Isa. be.
3 sj); to see the glory of the Lord with which God hath crowned
him, for he is over them a righteous king taught of God. In his
days there shall be no unrighteousness in their midst; for they are
all holy, and their king the anointed of the Lord (xp"tt65 nipios, mis-
translation of nin' ri'B'D). He shall not trust on horses and riders
and bowmen, nor heap up gold and silver for war, nor put his confi-
dence in a multitude for the day of war. 'The Lord is king,' that is
his hope. ... He is pure from sin to nile a great people, to rebuke
governors and destroy siujiers by his mighty word. In all his days
he is free from offence against. his God, for He hath made him
strong by the Holy Spirit. . . . His hope is in the Lord ; who
car. do aught against him ? Strong in deeds and mighty in tlie fear
of the Lord, he feedeth the flock of the Lord in truth and righteous-
ness, and suffereth not one of them to stumble in the pasture. . . .
So it bescemeth the king of Israel whom God hath chosen to lead
the house of Israel. . . . God hasten His mercy on Israel to
deliver ihem from the uncleanness of profane foes. The Lord is our
king for ever and ever." — Pso.U. Sol. xvii.
This conception is traced in lines too firm to be those of a
first essay; it had doubtless grown upas an integral part of
the religioiw protest against the Hasmonjeans. ■ And while
the polemical motive is obvious, and the argument from
prophecy against the legitimacy of a non-Davidic d_\niasty
is quite in the manner of the scribes, the spirit of theocratic
fervour which inspires the picture of the Messiah is brc ader
and deeper than their narrow legalism. In a word, the
Jewish doctrine of the Messiah marks the fusion of
Pharisaism with the national religious feeling of the
56
l'^ E S — I\J E S
2iIac-:abeo revival. It is tins national feeling that, claim-
ing a loader against the Romans as ■o'ell as deliverance
from the Sadducee aristocracy, again sets the idea of the
kingship rather than that of resurrection and individual
retiiljution in the central place which it had lost since the
captivity. Henceforward the doctrine of the Messiah is
at once the centre of popular hope and the object of
theological culture. The New Testament is the best
evidence of its influence on the masses (see especiall}' Matt.
x.xi. 9) ; and the exegesis of the Targums, which in its
beginnings doubtless reaches back before the time of
Christ, shows how it was fostered by the Kabbins and
preached in the synagogues.^ Its diffusion far beyond
Palestine, and in circles least accessible to such idea.s, is
proved by the fact that Philo himself (De Prxm. et Poin.,
§ 16) gives a Messianic interpretation of Num. xxiv. 27
(LXX.). It must not indeed bo supposed that the doctrine
was as yet the undisputed part of Hebrew faith which it
became when the fall of the state and the antithesis to
Christianity threw all Jewish thought into the lines of the
Pharisees. It has, for example, no place in the Assiimptio
M'isis or the Booh of Jubilees. But, as the fatal struggle
with Rome became more and more imminent, the eschato-
logical hopes which increasingly absorbed the Hebrew
mind all group themselves round the person of thj
Messiah. In the later parts of the Book of Enoch (t!.e
"symbols" of chaps, xlv. sq.) the judgment day of the
Messiah (identified with Daniel's " Son of Man ") stands
in the forefront of the eschatological picture. Jos(3phus
(/?. J. vi. 5, § 4) testifies that the belief in the immediate
appearance of the Messianic king gave the chief impulse
to the war that ended in the destruction of the Jemsh
state ; after tho fall of the temple the last apocalypses
{Bdruch, 4 E^-a) still loudly proclaim the near victory of
the God-sent king ; and Bar Cochebas, the leader of the
revolt against Hadrian, was actuaUy greeted as the jilessiah
by Rabbi Akiba (comp. Luke xxi. 8). These hopes were
again quenched in blood ; the political idea of the Jlessiah,
the restorer of the Jewish state, still finds utterance in the
daily prayer of every Jew (the Sh'mune Esre), and is en-
shrined in the system of Rabbinical theology ; but its his-
torical significance was buried in the ruins of Jerusalem.^
But the proof written in fire and blood on the fair face
of Palestine that the true kingdom of God could not be
realized in the forms of an eartldy state, and under the
limitations of national particularism, was not the final
refutation of the hope of the Old Testament. Amidst the
last convulsions of political Judaism a new and spiritual
conception of tho kingdom of God, of salvation, and of the
Saviour of God's anointing, had shaped itself through the
preaching, the death, and the resurrection of Jesus of
Nazareth. As applied to Jesus the name of Messiah lost
all its i)olitical and national significance, for His victory over
the world, whereby .He approved himself the true captain
of salvation, was consummated, not amidst the flash of
earthly swords or the lurid glare of the lightnings of Elias,
^ Tlie T.irgiimic pass.i^es tluit .speak of tho Slessiah are i-egi-stered
by Buxtorf, Lex. ChaM., s v.
' False Messiahs have continued from time to time to appear among
the Jews. Such was Sorenus of Syria {circa 7'20 A.D.). Soon after,
Messianio hopes were active at tlie time of tlie fall of the Oinoy-
yad-f, and led to a Rcrious rising under Abu 'Isa of Isp.ahan, wiio
callfctl himself forerunner of tlio Messiah. Tho false Messi.ah D.ivid
Alrni (Alroy) appeared among tho warlike Jews in Azerbijan in the
mi'ldle of the V2.]A\ century. Tho Messianic claims of AbraK.im Abn-
lalia of Saragossa (bora 1240) had a cabalistic basis, and tlie same
studies enconraged tho wildest hopes at a later time. Thus Abarbanel
calculated the coming of tho Messiah for 1503 A.D. ; the year 1500
was in many places observed as a preparatory season of penanc« ; and
throughout the 16tli century th« Jew3 were nuK-h stirred "and more
than one false Mcseiah appeared. For tho false Jlessiak Saljbathai,
see vol. xIL p. 681.
: but in the atoning death through which He entered into
the heavenly glory. Between the Messiah of the Jews
; and the Son of JIan who came not to be ministered to but
to minister, and to give his life a ransom for many, there
was on the surface little resemblance ; and from their
standpoint the Pharisees reasoned not amiss that the
marks of the Messiah were conspicnously absent from this
Christ. But when we look at the deeper side of the
iSIessianic conception in the Psalter of Solomon, at ithe
heartfelt longing for a leader in tho way of righteousness
and acceptance \\'ith God which underlies the aspira-
tions after political deliverance, we see that it ^Tas in no
mere spirit of accommodation to prevailing language that
Jesus did not disdain the name in which all the hopes of
the Old Testament were gathered up. The kingdom of
God is the centre of all spiritual faith, and the perception
that that kingdom can never be realized without a personal
centre, a representative of God v.'itli man and man with
God, was the thought, reaching far beyond the narrow
range of Pharisaic legaUsni, which was the last lesson of
the vicissitudes of the Old Testament dispensation, the
spiritual truth that lay beneath that last movement of
Judaism which concentrated the hope of Israel in the
person of the anointed of Jehovah.
It would carry us too far to consider in this place the details of
tlio Jewish conception of the Messiah and tlie Messianic times as
they appear in the later apocalypses or in liabbinical theology. See
for the former tho excellent summary of Scliiirei', XTUchc Zcit-
ijcschichte, §§ 23, 29 (Leipsic, 1874), and I'oi' tho latter, besides the
older books catalogued by Schiirer (of which ScUocttgen, Horse,
1742, and liertholdt, CUristologia Jvdxomtm, 1811, may be specially
named), Wcbcr, AUsynagogale Tlicologic (Leipsic, 1880). For the
whole Bubject see also Drunmiond, Th^ Jctcish Messiah (London,
1S77), and Kuenen, IteJifjion of Israel, chap. xii. For the Messianic
hopes of tho Pharisees and tlie Psalter of Solomon see especially
Wcllh.ausen, Pharisiicr unci Sailducaer (Greifswald, 1874). In its
ultimate form the Messianic hope of the Jews is tho centre of the
wdiole eschatology, embracing the doctiine of the last troubles of
Israel (called by tho Rabbins the "birth pangs of tho Messiah "),
the apjtearing of the anointed king, the annihilation of the hostilo
enemy, the return of tho dispersed of Israel, tho gloi-y and world-
sovereignty of the elect, the new world, the resurrection of the dead,
and tho last judgnicnt. But even the final form of Jewish thcologj-
shows much vacillation as to these details, especially as regards their
sequence and mutual relation, thiis betraying tho iuade(iuacy of the
hannonistic method by which they were derived from the OIJ
Testament and the stoi-my excitement in which the Jlessianic idea
was developed. It is, for example, an oj^n question among the
Rabbins whetlier tho days of the Messiah belong to the old or to
the new world (ntn dViVH or N3n Q^ivn), whether the resuirec-
tion embraces all men or only the righteous,- whether it precedes or
follows the Messianic age. Compare Millenxium.
"VVe must also pass over the very important questions that arise
as to the gradual extrication of the New Testament idea of tho
Ciirist from the elements of Jewish political doctrino which had
so strong a hold of many of the first disciples — the relation, for ex-
ap.;ple, of the New Testament Apocalypse to contemjiorary Jewish
tlionght. A word, however, is necessary as to tho Rabbinical doc-
trine of the Messiah who suffers ami dies for Israel, tho Messiah son
of Joseph or son of Ephraini, who in Jewish theology is distinguished
from and subordinate to tho victorious son of David, The devel-
ojied form of. this idea is almost ceitainly a product of tho polemic
with Christianity, in which tho Ilubbinswcre hard pressed byargu-
ineuts from passages {eepecinily Isa. liii.) which their own exegesis
admitted to be Messianic, though it did not accojit the Christian
inferences as to tho atoning death of the Messianic king. That tho
Jews in tlie time of Christ believed in o sulleriug and atoning
Messiah is, to say the least, unjirovf^d and highly improbahlo. See,
besides -tho ' books above cited, Do Wotte, Oj'nscula; AVUnscho.
Die Leiden dca iftmka, 1870. Tlic opposite argument of King, The
Ynflmt'on Zcchariah (Cambridge, 1SS2), App. A, does not really
prove more than that the doctrine of the Messiah 13en Joseph found
ponita of attachment in older thought. (W. E. S.)
MESSINA, a city and seajrort at tho north-east corner
of Sicily, capital of the province of the same name,'' is
^ The province occupies the north-oast comer of the island, and is
CO miles in length by 30 in breadth. It is chiefly occupied with moun-
tain ranges and valleys ; tlitro are few plains. Tlio lartjest ri'-er is tl' '
M E T — M E T
57
-utuated on the Straits of Messiua (at this point about
■4 niilea wide), 8 miles .north-west of Eeggio and 130
miles east by north of Palermo, in 38° 15' N. lat., lo° 30'
E. long. The town is built between the sea and a range
of sharp and rugged hills, called the Dinnamare, 3707
feet at their highest point. It runs in a semicircle round
the harbour, and presents a picturesque appearance from
the sea, as the houses rise in tiers upon the slope of a hill.
and behind are the wooded mountains.
Messina is the second town of Sicily in importance and iii
^rzK. Its population was 97,074 in 1850, 111,85-tia 1871,
and 126,497 in 1881. It is an archiepiscopal see, and has
a universitj-, founded by the Jesuits in 1548, with a public
library of 50,000 volumes.
The excellence of its harbour makes Messina an import-
ant trading town. The harbour is formed by a tongue of
low land which runs out from the shore in the form of a
ackle, and encloses a round basin, open to the north only,
■where the entrance channel is about 500 yards wide. This
basin is H miles in circumference, and is of such depth
that the largest vessels are able to use it. It is estimated
that 1 300 steamers, with a total of 1,000,000 tons burthen,
BJod 9000 sailing ships, with a total of 500,000 tons bur-
then, enter the port yearly. The exports of Messina consist
•chiefly of cranges, lemons, raisins, wiue, oil, liquorice, and
hides. ILfcreis no prominent manufacture; but silk stuffs
are made in considerable quantities. Many of the inhabit-
ants are engaged in fishing, chiefly for tunny. Sword-fish
also are captured with the haqjoon iu the Straits during
July and August. Coral fishery is a trade of the people.
The hills behind Messina produce a strong dark wine,
inferior to that which is. made in other parts of the
island.
Jlessina has few buildings of importance or antiquity.
Tlie sieges and earthquakes from which the town has
suffered destroyed most of its monuments. After the great
earthquake in 1783 the city was almost entirely rebuilt.
The cathedral, the principal building, is a church of the
Norman period. It was begun in 1098 by Count Roger
L, and finished by his son Roger IL The church is in the
form of a Latin cross, 305 feet long and 145 feet wide in
the transepts. The lower half of the facade is encrusted
"with slabs of red and white marble. It has three Gothic
pfcrtals, with pointed arches and rich ornamentation,
belonging to the period of the Anjou dynasty. Tljc nava
contains twenty-six columns of Egyptian granite, said to
have been brought from an ancient temple of Poseidon
which stood near the Faro. The mosaics of the apses date
from the year 1330. In the choir are tlie sarcophagi of
the emperor Conrad TV. (d. 1254), of AJphonso the Generous
(d. 1458), and of Antonia, widow of Frederick III. of
Aragpn. In 1254 the cathedral was seriously damaged by
Sre; in 1559 the campanile was burned down; in 1783
the earthquake overthrew the campanile and the transept.
Tlio building therefore offers a mixture of styles, — first
Norman, then Gothic, then Early Renaissance, finally
Barocco and-Modern Gothic.
The history of Messina begins very carlr. It is sai<l to have been
founded, on the situ of a more ancient Sicilian town, by pirates
fr'.m Cumse, in 732 B.C. It took its earlier name cf Zanclc (a
sickle) from the shape of its harbour. Tlio numljer of its iiihabit-
Jints was increased by an influx of ChalciJians uni'er Crat.cmenes :
nnd in 649 B.c. the town was sufficiently prosperous and populous
to establish a colony at Himera. The Samian's occuoieJ Zaucle for
» slort time after Miletus had been captured by the Persians in
491 B.C. In the following year the city fell iuto the har.Js of
j\naril.as, tyrant of KhegiuEi, who introduced a population of
Mcssenians, from Messenia in the Peloponnesus : and they changed
the jiarae of tho place to Messana, in the Doric pronunciation, to
Aicwtara. The chief towns are Messina. Castroreale, Mistretta.
J^iti, and Milazzo. Tl'.o ponulaSLoa ia 1S54 was 3S0,279, iu 1371
•i!!0,ii!9, .'..id in 1881 4fi7,iSi
remind them of their fatherland. The sons of Anaxilas wore ex-
pelled from the goverument of Messina in 166 B.f., and a republic
established ; and this government was continued until Messina
fell into the hands of the Carthaginians during their wai-a with
Diouysius the elder of Syracuse (396 B.C.). The Carthaginian?
destroyed the city ; but Dionysiiis recaptured aud rebuilt it.
During the next fifty years Messina changed mastei-s several times,
till Timolcon finally expelled the Carthaginians in 313 B.c. In the
wars between Agathocles of Syracuse and Carthage, Messina took
the side of the Carthaginians. Agathocles's mei-ceuaries, tho
Mamertines, treacherously seized the town in 2S8 B.c. uud held it.
They came to war n-ith Hiero II. of Sji-acuse, after Agathocles'a
death ; and Micro's allies, the Carthaginians, helped him to roduc;
3Iessina. The Mamertines appealed for help to Rome, whidi was
granted, and this led to a collision-.betwcen Eome ami Carth.ige,
which ended in the First Punie War. At the close of that wiir,~iu
241 B.C., Messina became a possession of the Romans.' During
the civil wars which followed the death of Julius Ca;sar, Messina
held \rith Sextus Pompeius ; and in 35 B.C. it was sacked ly
Octavian's troops. After Octavian's proclamation as emperor he
founded a colony here ; and Messina coiitinueil to flourish as a
trading port. In the division of the Koman empire it belonged to
the emperors of the East ; aud in 647 A.D. Belisarius collected
his fleet hero before crossing into Calabria. The Saracens took the
city in 831 A.n. ; and in 1061 it was the fii*st jiermanent conquest
made ui Sicily by the Normans under Roger d'Hauteville. In
1190 Richard Cceur de Lion with his crusaders passed tix moutha
in Messina. He fell out with Tancred, the last of thfe Hauteville
dynasty, and sacked the town. In 1194 the city, with the rest of
Sicily, passed to the house of Hohenstaufeu under the eni])eror
Henry VI., who died there in 1197. At the time of the Sicilian
Vespers (1282), which drove the French out of Sicily, Messin:i
bravely defended itself against Charles of Anjou, and repulsed liis
attack. Peter I. of Aragon, throuoh his commander Ruggicro di
Loria, defeated the French otf the Faro ; and from 1282 to 171-1
Messina remained a pos.tessiou of the Spanish royal house. In !."»71
the fleet fitted out by the Holy League against the Turk asseiubl.:d
at Messina, and in the same year its commander, Don John of
Austria, celebrated a triumph in the city for his victory at Lepanto.
Don Jolin's statue stands in the Piazza delP Annuziata. For one
hundred years, thanks to the favours and the concessions of Charles
v., Messina enjoyed great prosperity. But the internal quaiTels
between the Merii, or aristocratic faction, and the Jlalvezzi, or
democratic faction, fomented as they were by the Spaniards,
helped to ruin the city (1571-78). The Messinians suspected tlic
Spanish court of a desire to destroy the ancient senatorial consti-
tution of the city, and sent to France to ask the aid of LouLs
XIV. in their resistance. Louis despatched a fleet into Sicilian
waters, and tho French occupied the city. The Spaniards replied
by appealing to Holland, who sent a fleet under Ruyter into the
Mediterranean. The French admiral, Duquesne, defeated llii
combined fleet of Sjiain and Holland, but, notwithstanding tliis
victoiy, the French siuldenly abandoned itessina in 1678, and the
Spanish occupied the town once more. The senate was suppressed,
and Messina lost its privileges. This was fatal to the iroport;in<-c
of the city, and it nevrr recovered. In 1743 the plague caiTied oil
40,000 inhabitants. The city was partially destroyed by earth-
quake in 1783. During the revolution of 1848 against the Bourbons
of Naples, Messina was bombarded for three consecutive days. In
1854 the deaths from cholera numbered about 15,000. Garibaldi
lauded in Sicily in 1860, and Jlessina w.as the last city in the island
taken from tho Bourbons and made a nart of united Italy und.^r
Victor Emmanuel.
Messina was the birthplace ofrthe following celebrated men :
Dicaearchus, the historian {cir. 322 B.C.) ; Aristocles, the Peri-
patetic ; Euhemerus, the rationalist {cir. 316 B.C.) ; Stci'ano
Protonotario, Klazzeo di Ricco, and Tomniasodi Sa-^iso, poets of the
court of Frederick II. (1250 A.n.) ; and Antonello da Messina, the
painter (1447-99), five of whose works are preserved in the
I university gallery. During the 15th century the grammarian
Constantino Lascaris taught in Messina ; and Bessarion was for a
I time archimandrite there.
I METALLURGY, a branch of applied science whoso
■ object is to describe and scientifically criticize the methods
used industrially for the extraction of metals from their
ores. Of the large number of metals enumerated in the
handbooks of chemistry, the vast majority, of course, lie
outside its range ; but it is perhaps as well for us to point
out that in metallurgic discussions even the +erni
" metallic," as applied to compounds, has a restricted
meaning, being exclusive of all the light metals, although
one of these, namely aluminium, is being manufactured
industrially. The following table enumerates in the order
of their importance the metals which cur subject at pre.-eat
58
METALLURGY
's understood to include ; the second column in each case
gives the chemical characters of the native compounds
utilized, italics indicating ores of subordinate importance.
The term " oxide " must be understood to include carbon-
ate, hydrate, and occaaionaJly (when marked' in the table
with *'! sUicate.
VIetaL Character of Ores.
Iron Oxides, sulphide.
P \ Complex sulphides, also oxidea,
"^ \ metal.
„., i Sulphide and reguline metal,
»'>«■• i ehloride. ^
Gold' Reguline metaL
T J i Sulphide and basic-carbonate, sul-
^^"1 -i pLlc&c.
Zinc Sulphide, oxide.*
Tin Oxide.
Mercury Sulphide, reguline metal.
Antimony Sulphide.
Bismuth Keguline metal.
Nickel and cobalt Arsenides.
Platinum and platinum metals... Reguline.
Aluminium Oxide, * sodio-fluoride.
'We have separated the last two from the rest because
the methods used for their preparation are more of the
character of laboratory operations, and because we do not
mean to include these in our general exposition of metal-
lurgic principles. The history of metallurgy, up to the
most recent times, is obscure. It is only since about the
beginning of this century that the art has come to be at
all scientifically criticized ; and in the case of the most
important processes all that science has been able to do
has been merely to put her stamp upon what experience
has long found to be right. Great and brilliantly
successful scientific efforts in the synthetic line are not
wanting, but they all belong to recent times. Science, by
its very nature, aims at publicity ; empiricism at all times
has done the reverse ; hence a hiotory of the development
of the art of metallurgy does not and cannot exist. A
few historical notes on the discovery of certain of the useful
metals are given in the introduction to Metals (q.v.).
General Sequence of Operations. — Occa.sionally metallic
ores present themselves in the shape of practically pure
compact masses, from which the accompanying matrix or
" gangue " can be detached by hand and hammer. But
this is a rare exception. In most cases the " ore," as it
comes out of the mine, is simply a mixture of ore proper
and gangue, in which the latter not unfroquently predomi-
nates so much that it is not the gangue but the ore that
really occupies the position of what the chemist would call
the impurity. Hence, in general, it is necessary, or at
least expedient, to purify the ore as such before the libera-
tion of the metal is attempted. Most metallic ores are
specifically heavier than the impurities accompanying them,
and their purification may be (and generally is) effected
by reducing the crude ore to a fine enough powder to
detach the metallic from the earthy part, rfud then washing
away the la.tter by a current of water, as far as possible.
In the case of a " reguline " ore, such as auriferous quartz,
for instance, the ore thus concentrated may consist substan-
tially of the metal itself,- and require only to be melted
down and cast into ingots to be ready for the market.
This, however, is a rare case, the vast majority of ores
being chemical compounds, which for the extraction of
their metals demand chemical treatment. The chemical
operations involved may bo classified as follows : —
1. Fiery Operations.^The ore, along in general with
some kind of "flux," is exposed to the direct action of a
powerful fire. ■' The fire in most eases has a chemical, in
addition to its obvious physical function. It is intended
either to burn away certain components of the ore— in
which case it m'lst be so regulated as to contriin a suiiicient
excess of unbumed oxygen ; or it is meant to deoxidize-
( " reduce ") the ore, when the draught must be rest ricted
so as to keep the ore constantly ^^Tapped up in combustible
fkme gases (carbonic oxide, hydrogen, marsh-gas, ire).
The vast majority of the chemical operations of metallurgy
fall into this category, and in these processes other metal-
reducing agents than those naturall}' contained in the fire
(or wind) are only exceptionally employed.
2. Atnali/amalion. — The ore by itself (if it happens t>
bo a reguline one), or the ore plus certain reagents (if it
does not), is worked up with mercury so tliat the metal i.*
obt3,ined ultimately as an amalgam, which can be separated
m'echanically from the dross. The purified amalgam is
subjected to distillation, when the mercury is recovered as
a distillate while the metal remains.
3. Wet Processes. — Strictly spealdng, certain amalgama^
tion methods fall under this head ; but, in its ordinary
acceptance, the term refers to processes in which the metal
is extracted either from the natural ore, or from the ore as
it is after roasting or some other preliminary treatment, by
means of an aqueous acid or salt solution, and from this
solution precipitated — generally in the reguline form — ^bv
some suitable reagent.
Few methods of metal extraction at once yield a pure
product. 'What as a rule is obtained is a more or less
impure metal, which requires to be " refined " to become
fit for the market. 'We now pass to the individual con-
sideration of the several steps referred to.
Comminution of Ores. — Assuming the ore to be given in the shape
of large lumps, these must first be broken up into small stones (t.f'
about the size of those used for macadamizing a road) before they can
go to the grinding-mill. This formerly used to be done by hand-
work; nowadays it is preferably effected by means of aii American
invention called the stone-breaker (fig. 1). This con.sists essentially of
two substantial vertical iron plates ; one is fixed, the other is couuected
with an excentric worked by an engine so as to alternately dash against
and recede from the former. The lumps of ore, in passing through
this jaw-like contrivance, are broken up into smaller fragments fit for
Fia. 1.— .^ll.■ -io.-in tstom-Brcakei'.
the mill. For the production of a coarse powdtr revolving cylinders
are often employed. Two cylinders of equ.al diameter and length,
made of iron, steel, or stone, are suspended by parallel axes in close
proximity to each other. The widtn of the sUt between them can
de made to vary according to the requirements of the case. The
cylinders are made to revolve in opposite directions, so that the
stones when run into the groove formed by their upper halves are
drawn between them and are crushed into bits of a size dependinjr
on the least distance between the two surfaces. Exceptionally hard
stones might bring the machine to a standstill or 'cause breakages ;
hence only one of the'two axes of rotation is absolutely fixed ; the
cushions of the other are only held in relatively fixed positions,
each bet^veen a couple of guiding rails, by means of powerful springs
at their backs. The springs arc made of alternalo disks of india-
rub!; r .aid sheet iron, and yield appreciably only to very strong,
pressures. Wheanu excv'itionallyhai-d stoue romca on, tbcyyieli
M E T A L L U n G-Y
69
and alloir it to pass through uncrashed. Sometimes tiro sets of
cylinders are arranged one above the other, so that the grit from the
oj)per falls into the jaws of the lower set to receire further com-
mination. The diameter of the cylinders is from a foot to a yard,
their length from 9 inches to a yard, the velocity of a point on the
periphery a foot to a yard per second. The quantity of ore reduced
per hour per lioi-se-power is about 5 cubic feet for quartz or other
hard minerals, and about 14 cubic feet for minerals of moderate
hardness.
For the production of a rcl.itivoly line powder the pounding-mill
is frequently used, which, in its action, is analogous to « mortar and
pestle. The morUr is a rectangular trough, while the pestle is
replaced by a parallel sot of heavy metal or metal-shod beams,
which (by means of a revolving cylinder with cogs catching pio-
jections on the beams) are lifted up in succession and tuen
let fall by their own weight so as to pound up tlie ore in the trough.
Tlie ore is supplied from a prismatic reservoir with a sloping
bottom leading iuto a canal througli which the stones slide into
tlic trough. A current of water, which constantly flows into the
trough from below, lifts uji the finer particles and carries them
away over the edge of the trough into a settling tank.
The object pursuej'iu powdering an ore is to prepare it for being
purified by washing. But the velocity with whicli a solid particle
falls through water de|>ends on its size as well as on its specific
gravity — an increase in eitlier accelerating the fall ; hence, where
tlio dilfcrence in specific gravity between tlie things to be seprated
is small, the washing must be preceded by a separation of the ore-
powder into porlioiis of approximately enual fineness. This is often
elfected by ]>a»iug the ore through a system of sieves of different
width of ijK'sh superposed over one another, the coarser sieve
always occupying the higher jiositiou. Sometimes the sieves are
'made to "go dry," sometimes tliey arc aided in their action by a
current of water which, more effectually thau mere shaking, pre-
vents adherence of dust to coarser jiarts.
Another contrivance is the " Drum " (fig. 2). A long perforated
circular cylinder made of sheet-iron, open at both ends, is suspended,
in .1 sloping position, by a revoh ing shaft iwssing through its axis.
The size of the perforations is generally made to increase in passing
from the upper to the lower belts of the cylinder. While the drum
Fio. 2.- Drum.
is revolving, the ore, suspended in water, flows in at the upper end,
and iu travelling down it casts off first its finest and then its coarser
jiarts, the coarsest only reaching the exit at the lower end. Tlie
several grailes of jiowder jiroduced fall each into a separate division
of the collecting tank.
The drum, of course, is subject to endless modifications. A
very ingenious combination is H. E. Taylor's "Drum Dressin"
M.achinc " (lig. 3). It consists of three truncated cone-shapc3
hums D, fixed co-axially to the 5,imc horizontal revolving shaft,
li u 1 f \ 2,
are not perforated, but
are armed inside with screw-threads formed of strips of sheet metal
«ied edgeways to the drum. The ore grit to be dressed is placed'
in a hopper A, and from it, by a worm B filed to the revolviue
shaft, IS being screwed forward into a short fixed truncated cone C
projecting into the revolving drum No. 1, iuto which it flows in
a constant current. The rotary motion of the drum tends to
convev the ore along the spiral path prescribed by the screw-thread
towards the other end, and from it into drum No. 2, and so on.
But the ore in each drum meets with a jet of water E impelling
It the opposite way, and the effect is that, in each drum, tht
lighter parts follow the wafer, and with it run off over the
entrance edge to be collected in a special tank, while the coarser
parte roll down the spiral path toward the next drum to undereo
further parting. The tank or pit for drum 1 r-ceives the finest
and hghtest parte, that of dram 2 a heavier, that of drum 3 a
still heavier portion, while only the very heaviest matter finds
Its way out of the exit end of No. 3 into a fourth receptacle.
Of the large number of other ore-dressers, only two need be men-
tioned here.
The "Claosthal Turn-Table" consiste of a circular table, the sur-
face of which rises from the periphery towards the centre so as to
form a very flat cone of about 170°, which is fixed co-axially to a ver-
tical rotary shaft. At the apex of the Uble, surrounding the shaft,
but independent of its motion, there is a circular trough of sheet zinc,
divided into two compartmente ; one receives a stream of water
carrying the ore, the other a supply of pure water. A large annu-
lar trough of sheet zinc is placed below the periphery of the table
so as to receive whatever may tall over the edge. It also is divided
into compartments, as shall be explained further on. Supposing the
table to be at rest, a sector of about 60° of it would be constantly
run over by the ore-mud out of the first compartment of the upper
trough. This mud current would suffer partial separation into
heavier and lighter parts,— rich ore resting in the higher and
poorer in the lower latitudes, and a still poorer ore falling over the
periphery into the lower trough. The same happens with the
moving table ; only each sector of such partially analysed ore under-
goes further purification by passing tluough about 90° of water-
shower. After passing this, it mcete with a perforated fixed water-
pipe going up radially to about half the radius of the table. This
pipe also carries sweeping brushes, so that the belt of ore from the
lower latitudes of the Uble is swept off into the corresponding section
of the receiving trough. AVhat of ore remains on the higher laritudes
subsequently meets with a similar arrangement which sweeps it oB
into its compartment If the table turns from the left to the right,
and we follow the process, beginning at the left edge of the ore-mud
compartment, it will be seen that a fii-st sector of the receivin"
trough gathers the light dross, a succeeding one an intenncdiate
product, a third the most highly purified ore. The "intermediate"
is generally run into the ore-mud trough of a second teble to be
further analysed.
In the "Continuous Wash-Pumps" (Continuirliche Setzpumpe)
of the Harz, three funnel-shaped vessels (one of which is shown in
fig. 4) are set in a frame beside one another, but at different levels,
so that any overflow from No. 1 runs into No. 2 and thence into
No. 3. Each funnel communicates below with ite own compart-
ment of a common cistern.
Into each funnel a riddle
with narrow meshes is in-
serted somewhere near the
upper end, while, beside the
riddle, there is a pump of
short range, which, by
means of an excentric, is
worked so that the piston
alternately goes rapidly
down and slowly up. The
mode of working is best
explained by an example.
At Breinigerberg in Rhenish
Prussia the apparatus serves
to separate a complex ore
into the following four
parts, which we enumerate
in the order of their specific
gravities— (1) galena (the
heaviest), (2) pyrites, (3)
blende, (4) dross. Sieve
No. 1 is charged with
granules of galena, just
large enough not to slip
through the meshes. No. 2
similarly with granules of
pyrites. No. 3 with those of blende. The .crude ore-mud goes into
sieve 1 ; the jerking action of the pump alternately tosses the
particles up into the water and allows them to fall ; the heaviest
naturally come down first, but what is most striking is that
nothing will pass through the bed of galena but what is at least
as heavy as galena itself. In a similar manner No. 2 and No. S
Fio. i. — Continuous Wash-Pump.
60
M E T A L L U R (t i
funnels sift out the pyritos iinil the blende respectively, so that
Elmost iiotliiug but dross runs off ultimately. The apparatus is
said to do its work with a wonderful degree of precision, and of
course is susceptible of wider application, but it ceases to work
when the raw material is a slime so fine that the particles fall too
slowly.
Wodes of Producing High Temperatures. — Most of what is to be
said on this topic has already been anticipated in the articles
Flt.l, Fuenace, and Bellows ; but a few notes may be added
oti specially metallurgic points.
Furnace Materials. — In a metallurgic furnace tlic working parts
a: least must be made of special materials capable of withstanding
tlic very high temperatures to which they are exposed and the
action of tl'o fluxes which may be used. No practically available
material fully meets both requirements, but there is no lack of
iiurely fire-proof substances.
Of native stones, a pure quartzose saud.stone, free from marl,
may be named as being well adapted for the generality of structures;
but such sandstone, or indeed any kind of fire-proof stone, is not
always at hand. Wh;\t is more readily procured, and consequently
more widely used, is refractory brick, made from "fire-clay." The
characteristic chemical feature of fire-clays is that in them the clay
proper (always some kind of h'ydrated silicate of alumina) is associated
with only small proportions of lime, magnesia, ferrous oxide, or
other protoxides. If the percentage of these goes beyond certain
limits, the bi-ieks', when fetrongly heated, melt down into a slag.
The presence of fre? silica, on the other hand, adds to their refrac-
toriness. In tact the best fire-bricks in existenc* are the so-called
Dinas bricks, which consist substantially of silica, contaminated
only with just enough of bases to cause it to frit together on bein^
baked. Dinas briclcs, however, on account of their high price, are
reserved for special cases involving exceptionally high temperatures.
Amongst ordinary fire-bricks those from Stourbridge enjoy tho
highest reputation. It follows from what has just been said that,
in a metallurgic furnace, lime-mortar cannot be used as a cement,
but must be replaced by fire-clay paste.
lu the construction of cupels, reverberatory furnaces, &c. , only
tho general groundwork is, as a rule, made of built bricks, and this
groundwork is coated over with some kind of special fire-proof and
lux-proof material, such as bone-ash, a mixture of baked fire-clay
and cokes or graphite, or of quarts and very highly silicated slags, &c.
These beddings are put on in a loose powdery i'rnn, and then stamped
fast They offer the advantage that, when worn out, they are easily
removed and renewed. The powerful draught which a metallui'gic
fire needs can be produced by a chimney, where the fuel forms a
relatively shallow layer spread over a largo grating; but, when
closely-packed deep masses of fuel or fuel and ore have to be kept
ablaze, a blast becomes indispensable.
Chimneys. — The efficiency of a chimney is measured by the
velocity V with which the air ascends through it, multiplied by its
section ; andi the former is in roughly approximate accordance
with the fonnnla
V-^VZ^lT-ToVTo,
-.ffhere h stands for tho height of the chimney, g for the acceteration
of gravity (32'2 feet per second), and T and T^ for the absolute
temperatures (meaning tho temperatures counted from - 273' C.) of
the air within and the air without the chimney respectively, while
k is a factor meant to account for the resistances which the air, in
it.s progress through the furnace, &c., has to overcome. In practice
T is talteii .ts the mean temperature of tho chimney gases, which
rheorctically is not unobjectionable ; but the weakest point in the
formula is tho smallness and utter inconstancy of the factor k^
which, according to P^clet, generally assumes some value of the
r.o'.ver I, ^, &c. Yet the formula is of some use as enabling
l;i ; to see tho way in which V depends on h and (T - T„)/Tj con-
jointly,— to see, for instance, how deficient chimney height may be
'Compensated for by an increase of temperature in the chimney
gases, and vice versa.
DloKlng-Uaehinca. — Of tho several kinds of blowers described
under Bellows (7. v.), the *' fans " are the best means for producing
Urge volumes of wind of relatively small but steady pressure ;
"bellows" aro indicated in the case of work on a relatively small
.scale requiring moderate wind pressure; whilo tho "cylinder blast"
..omcs in where large masses of high-pressuro wind are required.
Two highly interesting blowing-machines, however, aro omitted in
•hat article, which may be sliortly described here.
The "Water Blast" (Wassortrommelgeblase) is interesting
historically, having been used motallurgically in Ilungtiry for
many centuries. A mass of water, stored up in a reservoir, is made
:o fall down continuously through a high narrow vertical shaft
iiaving air-holes at its upper end. Tho vortical column of water
sucks in air through these holes and carries it down with it into a
kind »t inverted tub standing in a reservoir kept at a constant
level. •> Air and water there seiiarate, tho former (lowing away
through a jiipe into a wind-box, fiom which it is led to its ucstina-
Tho "Cagniardellc" (figs. 5, 6), so called from its in'/cntor Ca^niaril
Latour, also utilizes water vo carry air, but in quite anotlu-r wiy. By
means of a round shaft passing through its axis, a cylindrical drum
of sheet-metal is suspended slantingly in a mass of water, so that the
lower end is fully immersed, while of the upper end the segment
above the upper side of the shaft is uncovered. The space between
«haft and drum is converted into a very vide screw-shapeii canal by
a band of slu'ct-metal hermctic?-lly fixed edgeways to the two. Both
tho top and the bottom end of the drum are partially closed by flat
Fig. 6.
to 65 per cent. ; with bellow?,
bottoms sohlcred or riveted to tho respective edges; tlie lower
one leaves a ring-sh.iped opening between its edge and the shaft,
which serves for the introduction of a fixed air-pipe bent so as to
i-each up to near the top of the drum's air-space ; in the upper
bottom three quadrants are closed, the fourth is open. Supposing
the screw-canal, traced from below, to go from the left to the right,
the drum is made to revolve in the same sens.", and the effect is that,
in each revolution, the screw-canal at its top end swallows a certain
volume of air which, by the succeeding entrance of the water — wliich,
of course, moves relatively to the screw
— is pushed towards and ultimately into
the air-space at the bottom end. The
Cagninrdelle yields a perfectly continu-
ous blast, and, as it is not encumbered
with any dead resistances except the
friction of the shaft against its bearmgs
(which can bo reduced to very little)
and the very slight friction of the water
against tho screw-canal, it utilizes a
very large percentage of the energy
speut on it This percentage, accord-
ing to experiments by Schwamlirug,
amounts to from 75 to 84-5; iu the
case of tho cylinder-blast it is
about 40 per ceut. ; witli the " 'Wasserti-ommelgeblase" 10 to 15 per
cent. Hence the " "Wassertrommelgeblase " stands last in relative
etficiencr ; but we must not forget that it alone directly utilizes
nativeener^y, while, in the cylinder blast, for example, 100 units
of work doSe by tho steam-engine involve a vastly greater eneigj
spest on th« engiue .as heat.
To maintain a desired temperature in a given furnace chargeil in
a certain manner, tho introduction of a certain volume of airper
unit of time i.s necessary. But this quantity, in a given blowing-
machine, is determined by the over-jiressuro of the wind, as
raeasurcd'Tiy a manometer, the velocity of the wind being approxi-
mately proportional to \/M/(B-H M), wheix' II stands for the height
of tho mercury-manometer, and B for that of the barometer.
Hence the practical metallurgist, in adjusting his blast, has nothing
to do but to seo that tho manometer shows the reading which, by
previous trials, has been proved to yield an adequate supply of wind.
Fuel. — In sonic isolated cases tho ore itself, by its combustion,
supplies the necessary heat for the operation to bo performed upon
it. Thus, for instance, the roasting of blackbaud iron-stone is
oifected by simply piling up the ore and setting fire to it, so that
the ore is at tho same time its own furnace and fuel ; in tho
Bessemer iirocess of steel-making, the burning carbon of the pig^
iron supplies tho heat necessary for its own combustion ; and a
similar process has been tried oxperimentallv, end not without
success, for the working up of certain kinds of [lyrites. But, as a
rule, the high temperatures required for the working of ores are pro-
duced by the combustion of extraneous fuel, such as wood, wood-
charcoal, coal, coke Of tlioso four, wood-charcoal is of tho widest
apidicability, but not much used in Britain on account of \\.»
liigh price. Iligh-eUsii coke or pure anthrncite, volsmc for volume.
METALLURGY
61
vts tlio liigliMt temperature. Wood or coal is indicntcd when a
\ luminous llame is one of the requisites. Olviousiy fuel of the
sr.mc kind auJ quality gives a higher calorific intensity when, before
use it is deprived by drying of its moisture, or wheu it is used iu
conjunctiou with a hot instead of a cold blast This latter prin-
ciple, as every one knows, is largely discounted in the manufacture
of pig-iion, where nowadays coal, with the help of the hot blast,
is made to do what formerly could only be effected with charcoal or
coke. For further in.forniulion sec Fuel and Inox.
ciiemical Operations. — In regard to processes of amalgamation
and to wet-way processes, we have nothing to add to what was given
in a previous paragraph ; '. wo therefore here confine ourselves, in
the main, to ))yro-cheniical operations.
The method to bo adapted for the extraction o! i E?'al from its
ore is determined chiefly, thougli not entirely, by the nature of the
non-metallic component with which the metal is combined. The
simplest case is that of the regulino ores where there is no non-
metallic element. The important cases are those of GoLi>, Bismuth,
and MEncunYte.D.).
Oxides, Hydrates, Carbonates, and Silicates. — All iron and tin ores
proper fall under this heading, which, besides, comprises certain ores
of copper, of lead, and of zinc. In any case the first step consists
in subjecting the crude ore to a roasting process, the object of which
is to remove the water and carbonic acid, and burn away, to some
extent at least, what there may be of sulphur, arsenic, or organic
matter. The residue consists of an impure (perhaps a very impure)
oxide of the respective metal, which iu all cases is reduced by treat-
ment with fuel at a high temperature. Should the metal be present
in the silicate form, lime must be added in the smelting fo remove
thp silica and liberate the oxide.
In the case of zinc the temperature required fur the reduction lies
above the boiling point of the metal ; hence the mixture of ore and
reducing agent {cljarcoal is generally used) must be heated iu a
retort combined with the necessary condensing apparatus. In all
the other cases the reduction is effected in the fire itself, a tower-
shaped blast furnace being preferably used. The furnace is charged
with alternate layers of fuel and ore (or rather ore and flux, see be-
low), and the whole kindled from below. The metallic oxide,
partly by the direct action of the carbon with which it is in contact,
but principally by that of the carbonic oxide produced in the lower
strata from the oxygen of the blast and the hot carbon there, is re-
duced to the metallic state ; the metal fuses and runs down, with
the slag, to the bottom of the furnace, whence both are withdrawn
by the periodic opening of plug-holes provided for the pui-pose.
). Sulphides.— Inn, copper, lead, zinc, mercury, silver, and anti-
mony very frequently present themselves in this state of combin-
ation, as components of a very numerous family of ores which may
be diridcd into two sections : (1) such as substantially consist of
simple sulphides, as iron pyrites (FeSj), galena (Pb.S), ziuc blende
(ZnS), cinnabar (llgS) ; and (2) complex sulphides, such as the
various kinds of sulphureous copper ores (all substantially com-
pounds or mixtures of sulphides of copper and iron) ; bournonitc,
a complex sulphide of lead, antimony, and copper ; rotligiltigerz,
sulphide of silver, antimony, and arsenic ; f^ihlerz, sulphides of
arsenic and antimony, combined with suliihides of copper, silver,
iron, zinc, mercury, silver ; and mixtures of these and other sul-
phides v ith oue another.
In the treatment of a sulphureous ore, the first step as a lule is
to subject it to oxidation by ronstiu" it in a reverberatoiy or other
furn.ace,' which, in the fust instance, leads to the buniing away of at
least part of the arsenic and part of the sulphur. Tlie elfect on the
several individual metallic sul[iliides (supjiosing only one of these
to be present) is as follows : —
M 1. Those of silver (A"jS) and mercury (HgS) yield sulphurons
acid gas and metal ; in the case of silver, sulphate is formed as an
iutenuediate product, at low temperatures. Jletallic niercur}*, in
the circumstances, goes off as a vapour, whicli is collected, and con-,
denscd ; silver remains as a regulus, but pure sulphide of silver is
tliardly ever worked.
52. Sulphides of iron and zinc yield the oxides Fe^Oj and ZnO as
final products, some basic sulphate being formed at the earlier stages,
. more especially in the case of zinc. The oxides can be reduced by
carbon.
> 3. The sulphides of lead and copper yield, the former a mixture
of oxide and normal sulphate, the latter one of oxide and basic
sulphate. Sulphate of lead is stable at a red heat ; sulphate of
copiier breaks up into oxide, sulphurous acid, and oxygen. In
ifiractice, neither oxidation process is ever puslied to the end ; it is
sto])ped as soon as ^he mixture of roasting-iuoduct and unchanged
sulpnide contains oxygen and sulphur in tlie ratio of O2 : S. 'I'he
access of air is then stopped and the whole heated to a higher
t»-niperature, when the potential SO^ actually goes oflf as sulphurous.
acid gas and the whole of the metal is elindnated as such. This
method is largely utilized in the smelting of lead (from g.alena) and
of copuer from Vopper pyrites. In the hitter case, however, the
V
' K^niip^c! arc giv
See also SlL^*E^«
sulphide Cii^S has first to bo produced from the ore, which is done
substantially as follows. Tlie ore is roasted with silica until a
certain proportion of the sulphur is burned away as SO.j, while a
corresponding proportion of oxygen has gone to "the metal ]»rt of
the ore. Kow it so happens that copper has a far greater athnity for
sulphur than iron has ; hence any locally produced oxide of copper,
OS long as sufficient sulpliido of iron is left, is sure to be reconverted
into suliiliido, and the final result is that, while a large quantity of
oxidized iron passes into the slag, all the copper and part of the iron
separate out as a mixed regulus of CUgS aaJT FeS (" mat"). This
regulus, by being fused up repeatedly with oxidized copper ores or
rich copper slags (virtually with CuO and silica), gradually yields
up the wliole of its iron, so that ultimately a regulus of pure subsul-
phide of copper, Cu„S ("fine mat"), is obtained, whicii is worked
up for metal as above explained.
•1. Suljihide of antinioji}', when roasted in air, is converted into
a kind of alloy of sulphide and oxide ; the same holds for iron,
only its oxysulphide is quite readily converted into the pure
oxide FcaOg by further roasting. Oxysulphide of antimony, by
suitable processes, can be reduced to metal, but these processes aio
rarely used, because the samo end is far more easily obtained bv
"precipitation," i.e., withdi-awing the sulphur by fusion witli
metallic iron, forming metallic antimony and sulphide of iron.
Both products fuse, but readily part, because fused antimony is
far heavier than fused sulphide of iron is. A precisely similar
method is used occasionally for the reduction of lead fiom galena.
Sulphide of lead when fused together with metallic iron in tho
proportion of 2Fe :lPbS yields a regulus ( = lPb) and a "mat"
FcoS, which, however, on cooling, decomposes into FeS parts of
onlinary sulphide and Fo parts of finely divided iron. What wo
have just been explaining are only two special cases of a moj-c
general metallurgic proposition. According to Fournet, any one of
the metals copper, iron, tin, zinc, lead, silver, antimony, ai;^enic,
in general, is capable of desulphurizing or precipitating (at least
partially) any of the others that follows it in the series just given,
and it does so the more readily and completely the greater the
nuu^bcr of intervening terms. Hence, supposing a complete mix-
ture of tliese metals to be melted down under circumstances admit-
ting of only a partial sulphuration of the whole, the cop|ier has the
best chance of passing into the " mat," while the arbcuic is the
first to be eliminated as such, or, in the Jircseuce of oxidants, as
oxide.
Arsenides. — Although arsenides are amongst the c<)nmonest
impurities of ores generally, ores consistiug essentially of arsenides
are comparatively rare. Tlie most important of them arc certain
double arsenides of cobalt and nickel, which in ]iracticc, however,
are .always contaminated with t^e ai-senidcs or other coiuiiounds of
foreign metals, such as iron, manganese, kc. The general mode of
working these ores is as follows. The ore is firet roasted by itself,
when a part of the arsenic goes off as such and as oxide (botli
volatile), while a complex of lower arsenides remains. This residue
is now subjected to careful oxidizing fusion in the presence of glas^
or some other fusible solvent for metallic bases. The ell'ect is that
tlio several metals are oxidized awiiy and pass into the slag (as
silicates) in the following order, — first the manganese, secondly the
iron, thirdly the cobalt, lastly (and very slowly) tho nickel ; and
at any stage the as yet unoxidized residue of arsenide assumes the
form of a fused regulus, which sinks down through the slag as a
"speis." (This tenii, as will readily be understood, has the same
meaningin referencctoarsenidesas"mat" hasinrcgardto sulphides.)
By stopping the process at the right moment, we can juoduce a
speis whicli contains only cobalt and nickel, and if at tliis stage
also the flux is renewed we can further produce a speis which con-
tains only nickel and a slag which substantially is one of cobalt
only. The composition of the speises generally varies IVom AsMcj..
to AsJIe,., where " ile " means one atomic weight of metal in toto,
so tliat ill general lSIe-a:Fe + t/Co-h:iri, where z-Hi/H-:-l.^^ The
siliceous cobalt is utilized as a blue pigment called " smalte"; the
nickel-speis is worked up for metal, prefer.aljly by wet processes.
Minor Itcmjcnts. — Besides the oxidizing and reducing agents natu-
rally iiresent in the fire, and the "fluxes" added for the production
of slags, there are various minor reagents, of whicli the niorc im-
portant may bo noticed here. One— namely, metallic iron as a
desnliihurizer-li.is already been referred to. s •'
Oxide of lead. I'bO (litharge), is largely used as an oxidizing agent.
At a red heat, when it melts, it readily attacks all metals, except
silver and gold, the general result being tho formation of a mixed
oxide and of a mixed regulus, a distribution, in other words, of
both the lead and the metal acted oil between slag and regulu?.
More important and more largely utilized is its action on metallic
sulpiiidcs, which, in general, results in the formation of three
things besides sulphurous acid gas, viz., a mixed oxide slag includ-
ing the excess of litharge, a regulus of lead (which may include
bismuth and other more readily reducible metals), and, if the
lilli.argc is not sufTicient for a complete oxidation, a "m.it"
comprising the more readily sulphurizable niet-iU. Oxide of lead,
'being a niost powerful solvent for metallic oxides gener.illy, is also
62
krgely ns.d for the separation of silver or gold from base n.etallio
Metallic leaa is to metals generally what oxide of lead i, to
iretall c oxides. It accordingfy ia available as a solvent fVr 1 !
7s ',f or^ "r"'," P"-'-'- "f -<«^' d.ffused thrTugho t a Tj^l
01 slag or other dross, and uniting them into one r^ulus This
naturally eads us to consider the process of "cu ellatbn " wh o
discounts the solvent powers of both metallic iS a^id t's S
This process serves for the extr^iction of gold and silver from t W
^oys with base metals such as copper, antimony Lc The fir t
aten s to fuse up the alloy with a certain proportion of lead wMcl
8 determined by the weight of base metil to be eirm nakd and
la always sufficient to produce a lead-alloy of low fusin" po"nt Vhi,
alloy IS heated on a sUllow dish-shaped bed of bon? ea thto red
ness. and at this temperature subjected to the action of air The
CcTsir. ■: sZra^rgQ^nT/'Krtr'^-^^-f '"^^
t^^^T- "-f °"=--- -
carbon of the pig into carbonic acid, while the metal of the
reagent becomes iron and FeO or MnO resnectivelv tip '■,
rriiS^-^tii^'-Sa^si^ir-^--
of tl'.^^/^f"'i'^?'l=' i^PT'^yrf for the preliminary concentration I
tLlTH%tt1irr hfh:?'™lelT,"ont=haTfi I^ ^S" ''
which reduces part of the metairoxiX^pTesen' ° The^ gofd" and
iilETALLURGY
o'i^i^e^i:.'' OxTdtVcale!n°'?r r-""^*" '"^'^' '^''' '"»"g^"0'"
^rfs^^s;;-^--"----^-
sSf^:?r^;^t^:?45P"=?^"'(ca^:s!
stated in an i. fmUe numlllr '""".P"^"}™ "f « silicate can be
of fo.mulat"on heir Su«s .h?^;'' •j'^.'here must be one n.ode
I mode adapted by mc aIlur»U,. 1° '^?,""P «' '"nis. The
we start with tlfeTuant tf r T'"""?- '''".""' ''°"™'''S- "
H,SO,of sulphmic^"aew7t"=,Lr tira'"tn?„?'''T '■';? 1"?"'"^
I normal salt we renuire sn!-!,, '^"".. r? convert either into a
H. of the acireoZ telv7l\?"f''"'/ f ,][''' ^' 'V" '=°'>vert the
does so is that containinVo^! V •' ''" ',""■ q'"">'i<yof l>ase that
is reasonab to define the o"anHi'°rn'"r'' "'' "^^W"- Henceit
CaO of lime, M^ of ma'n'esia fvn ,V "' ^"""'V ^"=0 "^ ^'"^''.'
of alumina, iFero/.ftolof eni. »' ^"^"^''^■Je, JAIA(-alO)
equivalent ■■^;iZ aL° iCreft" Le lo'^iHc^'Xr'T 'f' ,"°"^
ol.aracteristically indefinite basiStv M , 'r "'"">"el' sil.ca has a
pounds of silicates of AlO or Fe O InT f""? ",' ""r"^'' ""■ '^<'"'-
(CaO, .c), hence their gt^^"!, To'^^^isit":;-;'""'" °' '™'°"^"
follwLgtot:'f'ls:i^yi,,g:!;'d\t.-n"^'" .o. understand the
*■ ^"y"'K anrt naming composition in silicates.
uoite witL what islejror' rot^o^ii; i^droT ron (F I,'
selec ed as to convert the gangue into a fusible ■■ shi"wl,;h
readily runs down through the fuel with the reL, 1,„ ,J^^' .
.ts reduction thuS be prevented or Retarded S-.^^ the slag and
mightbe inclined to tlfink, rnLssaryevil if f X T ""> ''%'""
little tenden'S^o^Sistire^baJc'^xd^'^.rra: limbic V'°^l '
fui of b 'si Vu^s [rr't^ "^"^ ^^'-^ •" ''^ "- ■"-' p""-
The names are the metalluigic ones ■ scicntin,-,>li»„.i=. i • .
i^^/:M£i.^i2^ni'^^^,-?---:-;i,i;a^r^
silicate asafunction of ^,i,andof the natureoftheindividualbases
t.kingsio,.„Meo,;h;;tran:e:n r-^^i-^kie j^';::;:^
LToIm.""-" P''.';?"^' ^'"S. " ""-St have tie proper value ' Un
and Its meta (iron in our examnle) contaminate the regulus In
ox^^es"of r * '= ^,™""" ""''" ^'»"'^^'°"- " '» -°^"' »°t ' g that
oxides of lead and copper are more readily reduced to metals than 1
o^doof uo» Fe,0, is to FeO, the latter more readily Jo FcO {ban 1
sill;Iteat2"5V "'"' "" "■'""™"= "^"^ =" 2100- C.!Te b?:
sn|s^^utr;^^Xeutirji.^t '"-^"'-^ -^ -^
regr tS::^^^::^::,';:^ -i^^^^'^'o t..i,icate is ydow or
I i.J.,ij ,." ,1.5 c.,0 '^^ '*""' <'-i.-'>. ao b,i„g .]„^
; iX"i;r;,:'!,rJi.7.'',".c '"""'■'' '"■•'*''"'='■"•■
caii!i\:[::^v?onr!hrof'ti:rcrp°L',rt: Tn"'" ^"-'^ """<>' •»■
than cither of the latter «-o In, ,?^' .'".'"""y "^" i' is lower
.^.Ueatcs.se,-l\?:^leat^^l°^^-^-^-:^^.
ti.silicate combinations melt hrgr^yVlassc" "riL" e'h "f ll'
lime, and so, in a more limited sense do feiVj*^?'" ""' ''•"
r:T"trc^rthe'!n"e™t- -"'^^ t° >-' do„"f ii'r „r.
■ t, nenr^^the^meantim^^ metal^^urgist has, for hia
' Fcir slips contain more lion traces of .tkuUcj.
M E T — M E T
63
coiSnnce, to rely on the very nameroiis analyses which have been
made of slags actually produced (by the rule of thumb) in successful
metiUurgical operations. For some of such slags also Plattner has
determined the fusing points He found for (1) Freiberg lead slag,
^KO, 3alO, 8SiOj ; oxygen-ratio, 3:4; melting-point at 1317° C. ;
(2) Freiberg crude slag, 15R0, 3aI0, ISSiOj ; oxygen-ratio, 1 : 1 j
melting-point at 1331° C. ; (3) Freiberg black-copper slag, 24FeO,
AljOj, ISSiO, ; oxygen-ratio, 9:10; melting-point at 1338° C. ;
(4) High-fiirnace slag, 6CaO, 3alO, OSiO,; oxygenr ratio, 1:1;
melting-point at 1431 C
Jlelalliirgic Assaying. — To assay an ore originally meant to
execute a set of tentative experiments on a small scale in order to
find out the proper mode of working it practically. But nowadays
the term is always used in the sense of an analysis carried out to
determine thT) money -value of an ore. For this purpose, in many
cases it is sufficient to determine the percentages of the metals for
which the ore is meant to be worked. But sometimes nothing
short of a complete analysis will do. This holds more especially of
ores of iron. As this metal is cheap, the value of an ore containing
it depends as much on the nature and relative quantities of the im-
purities as on the percentage of metal. The proved absence of sulphur
and phosphorus may be worth more than an additional 5 per cent,
of iron, which latter again woulil perhaps not compensate for ths
proved presence of a large percentage of uncombined silica.
An assay to be of any value must start with a fair samph
object of sale. The fulfilment of this condition in all <
dinicult. The general method is, from say a given ship load of ore,
to take out (say) half a ton of ore from a large number of different
places and to crush this large sample into small fragments of uniform
size, which are well shovelled up together. From different parts of
this 6re-heap a sample of the secoml order — amounting to, say, 20
lb — is then drawn, and rendered more homogeneous by finer powder-
ing and mixing. From this sample of the second (or perhaps from
one of the third) order quantities of 1 or 2 lb are bottlecf ujx for
assaying. At the same time the moisture of the ore is determined,
on a large scale, by some conventional method, such as the drying of
1 or 2 lb in an open basin at 100° C, and weighing of the residue as
dry oi"e. This is done at the sampling place by the lirms concerned.
The assayer further pounds up and mLxes his sample, and then pro-
^ceeds to determine the percentages of moisture and metal in his own
■way. He has always the choice between two methods, the dry and
the wet. For the majority of gold or silver ores, and for cobalt and
nickel ores almost as a rule, certain dry-process tests are preferred
as the most exact analytically. In almost all other cases it may be
said that the wet method is susceptible of the higher degree of pre-
■cision, yet even in some of these cases the old dry-process tests are
preferred to the present day. For instance, all copper ores in the
British Isles are sold by the result of the Swansea assay, a kind
of imitation of the process of sulphureous copper-ore smelting; and
this, singularly, is adhered to even in the case of such cupriferous
materials as are worked by the wet way, although the Swansea
assay is well known to lose about 1 per cent, of the copper present.
A copper-smelter therefore had better buy 5 per cent, than 10 per
cent, copper-pyrites cinders, because in the first case he pays only
for four-fifths, while in the latter he must pay for nine-tenths of
the copper present To compensate for this anomaly, empirical
■methods have been contrived for calculating prices. (W. D.)
METALS. The earliest evidence of a knowledge and
use of metals is found in the prehistoric implements of
the so-caUed Bronze and Iron ages. In the earliest periods
• of written history, however, we meet with a number of
metals in addition to these two. The Old Testament
mentions six metals — gold, silver, copper, iron, tin, and
lead. The Greeks, in addition to these and to bronze,
came also to know mercury ; and the same set of metals,
without additions, forms the list of the Arabian chemists
of the 8th and of the Western chemists of the 13th cen-
tury. During the 15th century Basilius Valentinus dis-
covered antimony ; he also speaks of zinc and bismuth,
but their individuality! was established only at a later period.
About 1730-40 the Swede Brand discovered arsenic and
cobalt (the former is not reckoned a metal by modern
chemists), while the Englishman Ward recognized the
individuality of platinum. Nickel was discovered in 1774
by Cronstedt, manganese in 1774 by Scheele. The
brothers D'EIhujart, in 1783, prepared tungsten; Hjelm,
ixi 1752, isolated molybdenum from molybdic oxide, where
• For further information on slags, see Berthier, Traite des essais par
" :'Pi» seche ; Winkler, Er/ahrunyssatze iiber die Bildung der
'x.i\'''-^:c,i, Freiberg, 1827 ; Plattner, Vorlesungm iiber allgemeine
!.:!:^;:'-'"uie, >.2B fg.i Percjj Metallurgy,
its existence had been conjecturally asserted by Bergmann
in^l781. .©Uranium, as a new element, was discovered by
Klaprothin 1789 ; but his metallic "uranium," after having
been accepted as a metal by all chemists until 1841, was
then recognized as an oxide by Pdligot, who subsequently
isolated the true metal. Tellurium was discovered by MiiUet
von Eeichenbach in 1782 (again by Klaproth in 1798);
titanium, by Klaproth in 1795 ; chromium, by Vauquelin
in 1797 ; tantalum, by Hatchett in 1801, and by Ekeberg
in 1802. Palladium, rhodium, iridium, and osmium
(which four metals always accompany platinum in its ores)
were discovered, the first two by Wollaston in 1803, the
other two by a number of chemists ; but their peculiarity
was established chiefly by Smithson Tennant.
After Davy, in 1807 and 1808, had recognized the
alkalies and alkaline earths as metallic oxides, the existence
of metals in all basic earths became a foregone conclusion,
which was verified sooner or later in all cases. But the
discovery of aluminium by Wohler in 1828, and that of
magnesium by Bussy in 1829, claim special mention.
Cadmium, a by no means rare heavy metal, was discovered
only In 1818; by Stromeyer.
Of the large number of discoveries of rare metals which
have been made in more recent times only a few can be
mentioned, as marking new departures in research or offer-
ing other special points of interest. In 1861 Bunsen and
Kirchhoff, by means of the method of spectrum analysis,
which they had worked out shortly before, discovered two
new alkali-metals which they called caesium and rubidium.'
By means of the same method Crookes, in 1861, discovered
thallium; Keich and Richter, in 1863, indium; and Lecoq
de Boisbaudran, in 1875, gallium. The existence of the
last-named metal had been maintained, theoretically, by
Mendelejeff, as early as 1871. The existence of vanadium
was proved in 1830 by Sefstrbm; but what he, and sub-
sequently Berzelius, looked upon as the element was, in
1867, proved to be really an oxide by Eoscoe, who also
succeeded in isolating the true metal.
The development of earlier notions on the constitution
of metals and their genetic relation to one another forms
the most interesting chapter in the histoiy of chemistry
(see Axchemy). What modern science has to say on tie
matter is easily stated : all metals properly so called (i.e.,
all metals not alloys) are elementary substances; hence,
chemically speaking, they are not " constituted " at all, and
no two can be related to each other genetically in any way
whatever. Our scientific instinct shrinks from embracing
this proposition as final ; but in the meantime it must be
accepted as correctly formulating our ignorance on the
subject. All metallic elements agree in this that they form
each at least one basic oxide, or, what comes to the same
thing, one chloride, stable in opposition to liquid water.
This at once suggests an obvious definition of metals as a
class of substances, but the definition would be highly
artificial and objectionable on principle, because when we
speak of metal3 we think, not of their accidental chemical
relations, but of a certain sum of mechanical and physical
properties which unites them all into one natural family.
What these properties are wo shall now endeavour to
explain.
AU metals, when exposed in an inert atmosphere to a
sufficient temperature, as.'.ume the form of liquids, which
all present the following characteristic properties. They
are (at least practically) non-transparent ; they reflect ligljj;
in a peculiar manner, producing what is called " metallic
lustre." When kept in non-metallic vessels they take tke
shape of a convex meniscus. These liquids, when exposeu
to higher temperatures, some sooner others later, pass into
vapours. What these vapours are like is not known in
jnan;r cases, since, as a rak, they can.be produced only at
64
METALS
vei-y high temperatures, i^recluding the use of transparent
vessels. Silver vapour is blue, potassium vapour is green,
many otlicrs (mercury vapour, for instance) are colourless.
The liciiiid metals, when cooled down sufficiently, some at
lower others at higher teiiiperatures, freeze into compact
solids, endojTCd-'with the (relative) uon-trans])arency and
the lustre of their liquids. These frozeii metals in general
form compact masses consisting of aggregates of crystals
belonging to the regular or rhombic or (more rarely) the
quadratic system. But in many cases the crystals are so
closely packed as to produce an apparent absence of all
structure. Compared with non-metallic solids, they in
general are good conductors of heat and of electricity.
But their most characteristic, though not perhaps their
most general, property is that they combine in themselves
the apparently incompatible properties of elasticity and
ligidity on the one hand and plasticity on the other. Xo
this remarkable combination ot jiroperties more than to
anything else the ordiiiary metals owe their wide applica-
tion in the mechanical arts. In former times a high
specific gravity used to be quoted as one of the characters
of the genus ; but this no longer holds, since w:e have come
to know of. a whole series of metals which float on water.
Let us now proceed to see to what degree the mechanical
and physical properties of the genus are developed in the
several individual metals.
Kon-Trdnsparenctj. — This, in the case of even the. solid
metals, is perhaps only a very low degree of transparency.
In regard to gold this has been proved to be so ; gold leaf,
or thin films of gold produced chemically on glass plates,
transmit light with a green colour. On the other hand,
those infinitely thin films of silver which can be produced
chemically on glass surfaces are absolutely opaque. Very
thin films of liquid mercury, according to Melsens, transmit
light with a violet- blue colour ; also thin films of copper
are said to be translucent. Other metals, so far as we
know, have not been more exactly investigated in this
direction.
Colour. — Gold is yellow ; copper is red ; silver, tin, and
!-ome others are pure white; the majority exhibit some
modification or other of grey.
Bejlexion of- Light. — Polished metallic surfaces, like
those of other solids, divide any incident ray into two
)iarts, of which one is refracted while the other is reflected, — ■
with this difference, however, that the former is completely
absorbed, and that the latter, in regard to polarization, is
quite differently affected.' The degree of absorption is
different for different metals. According to Jamin, the
remaining intensity, after one and ten successive perpen-
dicular • reflexions respectively from the metal-mirrors
named, is as follows (original intensity = 1) : —
1 s„...
Speculu
1 R.
n JIcL-il.
10 R.
Steel.
] R.
10 R.
IR.
10 R.
ReU
•!i29
•■178
•692
•035
•609
•007
Yellow
•905
•ang
•632
•010
•699
•006
Violet
•867
•242
•599
•006
•599
•006
This shows the great superiority of silver as a reflecting
medium, especially in the case of repeated reflexion.
Crystalline Form. — Most (perhaps all) metals are capable
of crystaUization, and in most cases isolated crystals can bo
produced by judiciously managed partial freezing. The
crystals belong to the following systems : — regular sydem
— silver, gold, palladium, mercury, copper, iron, lead ;
quadratic system — tin, potassium ; rhombic system — anti-
mony, bismuth, tellurium, zinc, magnesium.
Structure. — Perhaps all metals, in the shape which they
ass\ime in freezing, are crystalline, only the degree of
, ' Tliis ra.^y be the cause of the peculiarity of metallic lustre.
visibility of the crystalline arrangement is very different
in different metals, and even in the same metal varies
according to the slowness of solidification and othei-
circumstances.
Of the ordinary metals, antimony, bismuth, and zinc
may be mentioned as exhibiting a very distinct crystalline
structure : a bar-shaped ingot readily breaks, and the
crystal faces are distinctly visible on the fracture. Tin
also is crystalline : a thin bar, when bent, " creaks "
audibly from the sliding of the crystal faces over one
another ; but the bar is not easily broken, and exhibits an
apparently •non-crj'stalline fracture. — Class I.
Gold, silver, copper, lead, aluminium, cadmium, iron
(pure), nickel, and cobalt are practically amorphous, the
crystals (where they exist) being so closely packed as to
produce a virtually homogeneous mass. — Class II.
The great contrast in apparent structure between cooled
ingots of Class I. and of Class II. appears, however, to hz
owingchiefly to the fact that, while the lattercrystallize iutha
regular system, metals of Class I. form rhombic or quadratic
crystals. Kegular crystals expand equally in'all directions;
rhombic and quadratic ores expand differently in different
directions. Hence, supposing the crystals immediately
after their formation to be in absolute contact with ono
another all round, then, in the case of Class II., such con-
tact will be maintained on cooling, while in the case of
Class I. the contraction along a given straight \[u& will iu
general have different values in any two neighbouring
crystals, and the crystals consequently become, however
slightly, detached from one another. The crystalline
structure which exists on both sides becomes ^^sible only
in the metals of the first class, and only there manifests
itself as brittlenes.?.
Closely related to the stiucture of metals is tlieir acgrce-
of " pksticity " (susceptibility of being constrained into-
new forms without breach of continuity). This term of
course includes a-s special cases the qualities of " inallo-
atility " (capability of being flattened out under the-
hammer) and " ductility " (capability of being drawn, into-
wire) ; but it is well at once to point out that these two
special qualities do not always go parallel to each other,
for this reason amongst others that duciihty in a higher
degree than Malleability is determined oy the tenacity of
a metal. Hence tin and lead, though very malleable, are
little ductile. The quality of plasticity is developed ta
very different degrees in different metals, and even in the
same species it depends on temperature, and may be
modified by mechanical or physical operations. A bar of
zinc, for instance, as obtained by casting, is very brittle;
but when heated to 100° or 150° C. it becomes sufficiently
plastic to be rolled into the thinnest sheet or to be drawn
into wire. Such sheet or wire then remains flexible after
cooling, the originally only loosely coliering crystals having
got intertwisted and forced into absolute contact with one
another, — an explanation supported by the fact that rolled
zinc has a somewhat higher specific gravity (7"2) than the
original ingot (0^9). The -same metal, when heated to
205° C, becomes so brittle that it can be ])Owdcred in a
mortar. Pure iron, copper, silver, and other metnbi are
easily drawn into wire, or rolled into sheet, or flattened
under the hammer. But all these operations render the
metals harder, and detract from their plasticity. Their
original softness can be restored to them by "annealing,"
i.e., by heating them to redness and then quenching them
in cold water. In the case of iron, however, this applies
only if the metal is perfectly pure. If it contains a few
])arts of carbon per thousand, the annealing process, instead
of softening the metal, g ves it a " temper," meaning a
higher degree of hardness Mid elasticity (see below).
What we have called plasticity must not be mixed up
METALS
65
VitlT'thTlaotion ot softness, which means the degree of
facility with which the plasticity of a metal can be dis-
counted. Thus lead is far softer than silver, and yet the
latter is by far the more plastic of the two. The now
famous experiments of Tresca {Comptes Sendus, lix. 754)
show that the plasticity of certain metals at least goes
considerably farther than had before been supposed. He
operated, with lead, copper, silver, iron, and some other
metals. Round disks made of these substances were
placed in a closely fitting cylindrical cavity drilled in
a block of steel, the cavity having a circuiar aperture
of two or four centimetres below. By means of an
hydraulic press, applied to a superimposed piston, a
pressure of 100,000 kilos was made to act upon the disks,
when the metal was seen to " flow " out of tie hole like a
viscid liquid. In spite of the immense rearrangement of
parts there was no breach of continuity. What came out
below was a compact cylinder with^ a rounded bottom,
consisting of so many layers superimposed upon one
another. Parallel experiments with layers of dough or
sand plus some ^.connecting material proved that the
particles in all cases moved along the same tracks as
would be followed by a flowmg cylinder of liquid. Of the
better known metals potassium and Sodium are the softest;
they can be kneaded between the fingers like wax. AfteV
these follow first thallium aild then lead, the latter being
the softest of the metals used in the.arts. Among these
the softness decreases in about the following order : — lead,
pure silver, pure gold, tin, copper, aluminium, platinum,
pure iron. As liquidity might be looked upon as the ne
plus ultra of softness, this is the right place for stating
that, while most metals, when heated up to their melting
points, pass pretty abruptly from the solid to the liquid
state, platinum and iron first assume, and throughout a
long range of temperatures retain, a condition of viscous
semi-solidity which enables two pieces of them to be
" welded " together by pressure into one continuous mass.
Potassium Und sodium might probably be welded if their
surfaces could be kept clear of oxide.
According to Prechtl, the ordinary metals, in regard to
the degree of facility or perfection with which they can be
hammered flat on the anvil, rolled out into sheet, or
drawn into wire, form the following descending series : —
Bammering. Rolling into Sheet. Drawing into Wire.
Lead. Gold. Platinum.
Tin. Silver. Silver.
Gold.' Copper. , Iron.
Zinc. Tin. Copper.
Silver. Lead Goli
Copper. Zinc. Zinc.
Flatinam. Platinnm. Tin:
Iron. Iron. Lead.
To give an idea of what can be done in this way, it may
be stated that gold can be beaten out to leaf of the thick-
ness of 3g^oa mm.; and that platinum, by judicious work,
can be dirawn into wire ^10^0,^ mm. thick.
By the hardness of a metal we mean the resistance
which it offers to the file or to the engraver's tooL Taking
it in this sense, it does not necessarily measure, e.g., the
resistance of a metal to abrasion by friction. Thus, for
mstance, 10 per cent, aluminium bronze is scratched by an
edge-tool made of ordinary steel as used for knife-blades.
And yet it has been found that the sets of needles used
for perforating postage stamps last longer if made of
'aluminium bronze than they do it made of steel
' Elasticity. —All metals are elastic to this extent that a change of
form, brought aboat by stresses not exceeding certain limit values,
will disappear on the stress being removed. Strains exceeding the
," limit of elasticity " result in permanent deformation or (if suffi-
ciently great) in rupture. Where this limit lies is in no case pre-
cisely known. According to Wertbeim* (who has done more for
ocr knowledge of the subject than any one else) and Hodgkinson,
Annalet de Chimie tt de PTiyiigw
16-5
the real law seems to be pretty much as indicated by the two curves
on the accompanying diagram, where, in reference to a metallic
T\-ire, stretched by an ajppended weight, the abscissa always means
the numerical value P of the weight, the ordinate of the upper curve
the total elonga-
tion caused by P, Y
theordinateofthe
lower curve that
part of the elong-
ation which re-
mains when P is
removed, so that
the piece of the
ordinate between
the two curves
gives the tempor-
ary ("elastic") ex-
pansion. From
P-0 np to a
somewhat indefi- _
nite point(« or A) " *» —
both curves are nearly straight lines, the lower almost coinciding in
its beginning with the axis of abscissae ; from that point onwards
these two curves approach each other, ami at a short distance from
the point of rupture they rapidly converge towards intersection. For
any value of P which lies fairly on the safe side of A, we have ap-
proximately
9
where X means the elastic (or substantially the total) expansion, I
the length, and j'the square section of the wire or cylindrical bar
operated upon. The reciprocal of «(viz. E = l/c) is called the
"modulus of elasticity. "
iVertheim has determined this constant for a large number of
metals and alloys. He used three methods : one was to measure the
elongations produced, in a wire of given dimensions, by a succession
of charges ; the other two consisted in causing a measured bar to
give ona musical note by (a) longitudinal and (6) transversal vibra-
tion, and counting the vibrations per second. The following table
gives some of his results. Column 2 gives the constant E for
millimetre and kilogramme. Hence 1000/E is the elongation in
millimetres per metre length per kilo. Column 3 shows the charge
causing a permanent elongation of 0'05 mm. per metre, — which,
for practical purposes, he takes as giving the limit of elasticity;
column 4 gives the breaking strain. Values of E in square
brackets [ ] are derived from vibration experiments; the rest
from direct measurements of elongations. Numbers in round
brackets ( i do not necessarily refer to the same specimen as the
other data.
For Wire of 1 Square ram.
SectioT), Weight (in
Nam*.
E.
Kilos)
caubing
PennaiieDt
EIODgatioD
Breakage.
of irfj.-
Lead, drawn „ „..
1,803
e-25
21
1,727
1-8
f5;q
(2-45)
„ annealed »....„..
0-20
[5,757]
2-24
[4,777]
8,132
13-5
27
,, annealed «
6,585
3-0
10
7,358
7,141
11-3
2-6
29
16
„ .annealed , «
9,021
Zinc, ordinary, drawn- ._
8,785
0-75
13
„ „ annealed. «
[9,467]
100
PoUadium, draw-n -
18
9,789
Qiiijer5
27
Copper, draw-n „ , „....
12,449
12
40
, 10,619
17,0M
16,518
16,987
16,623
under 8
(26)
04)
80
S4
Platinam wire, medluin thickness, )
28
Iron,* drawn «.«
20,869
S3
20,7M
under 6
jx61
Nickel.s drawn „
7,040
Aluminiuni^ „
Aluminium bronze *„,„,. *..
10,700
BrassO „.
8,543
10,788
The above numbers may be assumed to hold for temperatures from
15** to 20° C. Wcrtheim executed determinations also at other teni-
peratures; but, as his numbers do not appear to reveal the true
2 From Do Brery. * Approximate, by H. St Clalr DevtMe.
♦ From deflexion o( hammered bar of 6 mm. tWcknesa, charjped in the middle *
determined by W. Dlttmar. *
» Composition, ZoCu, (Werthelm). < CoiDp<teItlon, Zh^CouNhj {Wcrtheim;^
6e
METALS
relationa between E and temperature, we quote tie results of
^ohlransch and Loomis, who found the following rf Litions between
the modulua E, for 0° C. and the value Ei for + C C, :^ —
Iron: Ei=£|,(l--000483l--00000()l?l').
Copper : E( =Eo(l - • 0O0-'i72 *- '00000028/2).
.Braas: E( = Efl(l--00O4S5 /--OOOOOiae^.
Thus, for these thieo metals at least, the value of E diminishes,
when temperature increases, at pretty much the same rate per
Ue-gree of temperature,
_ Specific OravUij.— This varies iu metals from -664 (lithium) to
^2*48 (osmium), and in one and the same species is a function
pf temperature and of previous physical^ ana mechanical treat-
cient. It has in general one value for the powdery metal as
pbtained by reduction of the oxide in hydrogen below the melting
Jroiut of the metal, another for the metal in the state which
It assumes spontaaeously on freezing, and this latter value agafn,
in geueral, is modified by hammering, rolling, or wire-drawing, &c.
These mechanical operations do not necessarily add to the density ;
ftamping, it is true, does so necessarily, but rolling or drawing
occasioually causes a diminution of the density. Thus, for
instance, chemically pure iron in the ingot has the specific gravity
i7-84J ; when it is rolled out into thin sheet, the value falls to
|7-6 ; when drawn into thin wire, to 775 (Berzelius). The follow,
ing table gives the specific gravities of all metals (except a few
Tery_rare ones) according to the most trustworthy modern de-
jtermiiations. Where special statements are not made, the numbers
t)iay bo assumed to hold for the ordinary temperature (16° to 17° or
^0°C. ), referred to water of the same tempei-ature (specific gravity
f= 1) as a standard, and to hold for the natural frozen metal,
' NamA ftf lU,.tnt
strontium
Aluminium, pure, Ingot
Ahimliilum, ordinary, liammcred
Gallium
Lanthanum..
Didymium...
Cerium
Antimony,..,
Chromium ...
Zinc, incot...
„ rolled o
Mmiganese..
Tin,.
crystallised by galvanic cur
rentftdm solutions
Indium
Iron, cliemlcally pure, ingot....,
„ thin sheet
„ wrdught, high quality
Klckel, ingot
Cadmium, insot
Iiammered
Cobalt ,
Uolybdenum, containing 4 to I
per cent.
Copper, natlvi
liismuth,,
■iilve
stamped
Leiid, very slowly frozen
',, qnlcitly dozen In cold watt
Palladium
Vhaillum
Rhodium
HutVnium
ilercury, Uiuld
„ solid
Tungsten, couipact, by tlj iiom
chioildo vupour
„ as reduced by hydro-
gen, powder -.
Uranium..
Guid, Ingot
,, stamped
,, powdler, precipitated by
ferroQs sulphate
Platlnt
Specldc Gravity
■9735
1 52
1-578
1-743
5-5
6-9
6-163
(il-2S
6 715 atl6-
6-81
6915
7-2
8-04 to 8-95
8-945
9-823 at 12'
104 to 10 6
10-57
1 1 -254
11-363
14 J9 below— 40'
16-64
18-33
19-505 at 13"
19-31 to 19 34
21-46
22-40
22477
Antbority,
Bunsen and Ua'^UieSeD,
Clarke-
Troost.
Itoscoe.
Lecoq de Bolsbaadran.
Hiliebrandt and Norton,
Marctiand and Scheerer.
Hohler. '
Kariten.
nicbter.
Schreder
Marchand and Scheerer,
WShlcr, 1855,
Roscoc,
Pi!ilgcrt, 1868,
Mattiilesen,
G, Rose,
Deville and Dobray,ie;C,
t Thermic Properties. — The specific heats of most metals have been
determined vei-y carefully by Ki-gnaiilt, The general result is that,
conformably with Dulong and IVtit s law, the "atomic heats" all
come to very nearly the same value (of about 6-4); i.e., atomic
weight by specific heat -6 4. Thus we have for silver by tlieoiy
6-4/108- -0593, and by experiment -0570 for^OUo 100° C.
The expansion by heat varies greatly. The following table giT^f
the linear expansions from 0° to 100° C. according tO Fizcaa {Complft
Hendua, IxviiL 1126), the length at 0" being taken as«nity.
Name of UetaL
Expansion
0- to lOO-.
Platlnuqi, cast ,. «,.„.„.„„ »,
Gold, ca.t _ _
■000 907
■001 451
-001 936
•001 708
■001 SG9
■001 !!8
■001 !oa
•001 no
001 C41
■001 2S9
■001 874
■002 269
■002 948
■002 905
-003 102
. -002 336
■001 879
■001 802
Copijer, artifirlal „ «..-.„.... „..,-
Iron, soft, as u»cd for eicctromagncta, ..-• «
„ reduced by hydrogen and com)K-e<sed...,»«...
Cast steel, Engllab annealed _ *...,
Bismuth, in tile direction of the axis „,.„
„ at right angles to a,'^ls „ „,„
„ mean expansion, calculated «.«.„
Tin. of Malacca, compressed powder „
Bronze (8C-3 per cent, copper 9-7 per cent tin, 40 per cent, zinc)
The coefficient of expansion is constant for such metals only as
crystallize in the regular system ; the others expand differently
in the directions of the different axes. To eliminate thi^ source
of uncertainty these metals were employed as compressed powders.
The cubical expansion of mercury from 0* to 100° C. is -018153
-nr'TTir (RegnauU).
Fusibilitii and VolaiiUty. — The fusibility in different metalfl
i3 very different, as shown by the following table, which,
besides including all the fusing points (in degrees C. ) of metals
which have been detennined numerically, indicates those of a
selection of other metals by the positions assigned to them in the
table. Of the temperatures given, those above (say) 500° 0. musx
be looked upon as rough approximations.
Kame of MetaL
Fusing roint
Authority.
Mercury
-S8-8
+ 26 to 27
301
38-5
62-6
965
1800
176
228
264
290
320
825
425
415
413
625
700
1,040
1,100
1.100
1,200
1.300 to 1,400
higher
1.400
l.COO
?
1,600 to 1,600
st wind-furnace
3.000
2,870
9 yet infusible.
B. Stewart.
Sctteiberff.
L. de Uolsbaodran.
Bunsen.
V
nichter(?)
Rudberg.
Lamy.
Ruillicrg.
renir>n,
Danicll.
roiilllet.
Pouillet.
Bccqaercl.
Pouillet.
Pouillet
heat. The foUowljig
Cesium ,.._
Putasslum „
Lithium _
Lend „
Incipient Red Heat „
MagncBlHm ., :...
Aluminium -
Urunlum .,
Pnlladlum Is barely fusible at the blghe
melt only lu the oxyhydrngcn flame; —
A/ax. Temp, of Oiyhydrogen Flame....
Osmium does not melt at 2,870', i.e., Is a
Of the volatility of metals we have little precise knowledge;
jnly the following boiling points are known numerically : —
Karac of MctaL
BoUUig PolDt
Authority. |
Mercury ~
357-3
8G0
1.040
below 1.040
above 1.040
Ripnault.
Devilk oDdTroost.
Dow'orand Dlr'tmar.
For practical purposes the volatility of metals may bo stated as
tol.ows:-
1, Distillable below redness: mercury.
2, Di.<tillable nt red heats : cadmium, alkali metals, zinc, mag-
nesium.
3, Volatilized more or lesa readily when heated beyond thoir
fusin;; points in ojieu crueibles : antimony (very rendily), lead,
biiiuutb, tin, silver. - ;
Huntcn, Jabtib./. Chem, 18C7, f. 41; PhU.JUaf., xlllT. 4
^
M E .T A L S
67
4. Barely so:. gold, (copper). -^ , ,
6. Practically Don-volatile : (copper), iron, nickel, cobalt^ «lu-
miniam; siiso lithiam, barium, strootium, and calcium.
I In the oxybydrogen flame silver boils, forming a blue vapour,
while platinum volatilizes slowly, aod osmium, though infusible,
very readily.
I Laitnt Beats of lAq^uef action — Of these we know little. The fol-
lowing numbers are due to Person — ice, it may be stated, being 80.
HebU.
Latent
Heal.
MctaL
Latent
Heat.
Mercury .....................
2-82
6-37
12-4
Cadmium ._
Sflver _
Zinc _
136
211
28-1
Bismatb ..,»......»
Of the latent heats of vaporization only that of mercnry has been
determined, — by Marignac, who found it to be 103 to 106 units.
Conductivity. — Conductivity, whether thermic or electric, is veiy
differently developed in different metals ; and, as an exact know-
ledge of these conductivities is of great scientific and practical
importance, much attention has been given to their numerical
determination. The following are the modes' in which the two
conductivities have been defined as quantities.
1. Thermic. — Imagine one side (1) of a metallic plate, D units
thick, to be kept at the constant temperature <„ the other (II) at
t^ After a suiEcient time each point between 1 and II will be at
a constant intermediate temperature, and in every nnit of time a
constant quantity Q of heat will pass from any circumscribed area
~ 1 1, according to the equation
,S(£r
S 00 I to the opposite area S
I is called the (internal) conductivity of the metal the plate is
made of. It is, strictly speaking, a fonction of <, and <,; but
within a given small interval of temperatures it may be taken as a
constant.
2. Electric. — When a given constant battery is closed successively
by different wires of the same sort, then, according to experience,
the strength I of the current (as measured for instance by the heat-
equivaleut of the electricity flowing through the circuit in unit of
time) is in accordance with the equation
A/l=l+rlls ,
where 1 is the length and s the square section of the wire, while A
13 a constant which, for our purpose, need not be defined in regard
to its physical meaning; r measures the specific resistance of the
particmar metal. Supposing a certain silver vrire on the one hand
and a certain copper wire on the other, when substituted for each
other, to produce currents of the same strength, we have
r,',/.,=r,;,/.,,
whence
r,/rj=j,V(<2'i)=i
where k is the computed value of the ratio on the iight-hand side.
Hence, _ taking r,, the resistance of copper, as unity, we have
r,=A, i.e., k gives us the specific resistance of silver, that of copper
being taken = 1. In this relative manner resistances are usually
measured, silver generally being taken os the standard of compari-
son. Supposing the relative resistance of a metal to be R, the re-
ciprocal l/R is called its "electric conductivity." For the same
metal R varies with the temperature, the higher temperature cor-
responding to the higher resistance. The following table gives the
electric conductivities of a number of metals as determined by
Matthiesen, and the relative internal thermic conductivities of
(nominally) the same metals as determined by Wiedemann and
Franz, with rods about 5 mm. thick, of which one end was kept
at 100° C, the rest of the rod in a " vacuum " (of 5 mm. tension)
at 12° C. Matthiesen's results, except in the two cases noted, are
from his memoir in Fogg. Ami., 1858, ciii. 428.
Copper, commerda], No. 3....^ «...
No. 2 „
,. chemlcallr pura, hard drawn..
Copper \..„
Gold, pure
n absolutely pure „ i
Pianoforte wire..
Iron rod.
Steel
Lead, pure
Platinum
Gennan silver ....
Blsmutli. „...
Aluminium
Mercui-
SUver, pj
pbie
Relative Conductivities.
•115 ,
210
•144 ,
JO-
■ifrn ,
173
•105 ,
20-7
•0767 ,
18^7
•0119 ,
13-8
•106 ,
19-6
■01C3 ,
22-8
Going by Matthiesen's old numbers, we iind them to agree fairly
with Wiedemann and Franz's tlievmic conductivities, whiih 6iipi>or»»
an ob\-ious and pretty generally received proposition. Miitlhic-
scu's new numbers for gold and copper, however, destroy the Jm^'
mony. j«
Magiutic Properties.— hoii, nickel, and cobalt are the onlj
metals which are attracted by the magnet and can become magnets
tliemselves. But m regard to their power of retaining their mag-
netism none of them comes at all up to the compound metal steel.
See Magnetism.
Chemical Changes^
The chemical changes which metals are liable to may be
classified according to the loss of metallicity involved in
them. We will adopt this principle and begin with the
action of metals on metals, which, as experience shows,'
always leads to the formation of truly metallic compovmcUt*
Any two or more metals when mixed together in the
liquid state unite chemically, or at least molecularly, in this
sense that, although the mixture, on standing (hot), may
separate into layers, each layer is a homogeneous solution ot
" aUoy " of, in general, all the components in one another.!
With binary combiuations the following two cases may
present themselves : — (1) the two metals mix permanently
in any proportion ; or (2) either of the two metals refuses
to take up more than a certain Uniit-proportion of the
other ; hence a random mixture of the two metals will, in
general, part into two layers, — one a solution of A in F,,
the other a solution of B in A. The first case presents
itself very frequently; it holds, for instance, for gold and
silver, gold and copper, copper and silver, lead and tin,'
and any alloy of these two and bismuth. Many other
cases might be quoted. A good example of the second
case is lead and zinc, either of which dissolves only a very
small percentage of the other. In the preparation of an
alloy we need not start with the components in the liquid
state; the several metals need only be heated together in
the same crucible when, in general, the liquid of the more
readily fusible part dissolves the more refractory compo-
nents at temperatures far below their fusing points. Molten
lead, for instance, as many a tyro in chemical analysis has
come to learn to his cost, readily runs through a platinum
crucible at little more than its own fusing point.
A homogeneous liquid alloy, when solidified suddenly,'
say by pouring it drop by drop into cold water, necessarily
yields an equally homogeneous solid. But it may not be
so when it is allowed to freeze gradually. If, in this case,
we allow the process to go a certain way, and then pour off
the still liquid portion, the frozen part generally presents
itself in the shape of more or less distinct crystals; whether
this happens or not, the rule is that its composition differs
from that of the mother liquor, and consequently from that
of the original alloy. This phenomenon of " liquation," as
it is csdled, is occasionally utilized in metallurgy for the
approximate separation of metals from one another ; ' but in
the manipulation of aUoys made to be used as such it may
prove very inconvenient. It does so, for instance, in the
case of the copper-silver alloy which our coins are made
of ; in a large ingot of such sterling silver the core juay,
contain as much as 0'3 per cent, of silver more than the
outer shell.
The existence of crystallized alloys, as the phenomenon
of liquation generally, strongly suggests the idea that .
alloys generally are mixtures, not of their elementary com-
ponents, but of chemical compounds of these elements with
one another, associated possibly with uncombined remnants
of these. This notion is strongly supported by the fact
that the formation of man^ aUoys involves an obvious
evolution of heat and a derfded modification in what one
would presume to be the properties of the corresponding
iJL??''"'''''' "^ '*"• ""^ declared by MattUescn to be more exact than the old
' A good illustration is afforded by the process of Pattinson as used
for concentrating the silver in argentiferous lead. See Lead.
68
E T A L S
mixttue. The ca?e of sodium amalgam may be quoted
as a forcible illustration. ^Vhat goes by this name in
laboratories is an alloy of two to three parts of sodium with
one hundred parts of mercury, which is easily produced by
forcing the two components into contact with each other
by meana of a mortar and pestle, when they unite, with
deflagration, into an alloy which after cooling assumes the
form of a grey, hard, brittle solid, although mercury is a
liquid, and sc-iium, though a solid, is softer than wax.
Similar evidence of chemical action we have in the cases of
brass (copper and zinc), bronze (copper and tin), aluminium
bronze (copper and aluminium), and in many others that
might be quoted. There are indeed a good many alloys
the formation of which is not accompanied by any obvious
evolution of heat or any very marked change La the mean
properties of the components. But in the absence of all
precise thermic researches on the sulgect we are not in a
jwsition to assert the absence of chemical action in any
case. Indeed our knowledge of the proximate composition
of alloys is in the highest degree indefinite — we do not
even know of a single composite metal which has been
really proved to bo an unitary compound, and hence the
important problem of the relation in alloys between pro-
perties and composition must be attacked on a purely
empirical basis. What has been done in this direction
is shortly summarized in the following paragraphs.
Colour. -^ilost metals are white or grey ; eo are the alloys of
these metals with one another. Gol.i alloys generally exhibit some-
thing like the shade of yellow which one would expect from their
composition ; its amalgams, however, are all white, not yellow.
Copper shows little tendency to impart its characteristic red colour
to its alloys with white or grey metals. Thus, for instance, the silver
alloy up to about 30 per cent, of copper exhibits an almost pure
white colour. The alloys of copper with zinc (brass) or tin (bronze)
are reddish-yellow when the copper predominates largely. As
the proportion of white metal increases, the colour passes succes-
sively into dark yellow, pale yellow, and ultimately into white.
Aluminium bronze, containing from 5 to 10 per cent, of aluminium,
is golden-yellow.
Plasticity.— This quality is most highly developed in certain pure
metala, notably in gold, platinum, silver, and copper. Of platinum
alloys little is known. The other three, on uniting with one
another, substantially retain their plasticities, but the addition of
any metal outside the group leads to deterioration. Thus, for
instance, according to Karsten, copper, by being alloyed mth as little
as 0'6 per cent, of zinc, loses its capability of being forged at a
red heat ; it cracks under the hammer. Antimony or arsenic to
the extent of 0-15 per cent, renders it unfit for being rolled into thin-
sheet or drawn out into fine wire, and makes it brittle in tho heat ;
O'l per cent, of lead prohibits its conversion into leaf.
Hardness, Elasticity, Taisile Strength,— In reference to these
qualities, we shall confine ourselves to some very striking changes for
the better which the metals (l)gold, (2) silver, (3) copper suffer when
alloyed with moderate proportions (10 per cent or so) of (1) cop-
per, (2) copprr, (3) tin, zinc, or alumluium respectively. Any of
those five combinations leads to a considerable increase in tho three
qualities named, although these are by no means highly developed
in the added metals ; most strikingly it does so in the case of alumi-
nium bronze (copper and aluminium), which is so hard as to bo
very difficult to file, and is said to bo equal in tensile streniTth
to wrought iron. To illustrate this we give in the following table,
after Matthiesen, the breaking strains of double wires. No. 23
gauge, in tb avoirdupois, for certain aUoys on tho ono hand, and their
components on tho other.
Mloyt.
efal, 12 per cent, of tin 80-00
o;'d?;!."V.::::::::":":;:::::::::::::'.::2oi25 ^ shmdora (22 camD gow 70-75
Silver i0-4fi )
riattanm ".'.".'.'.'.".".'.'.'.ii-so!^''^' ' °' '""'■■ i "' pl^ttaam ....75-80
Specific Oraviiy. — This subject has been extensively investigated
by Matthiesen, Culvert and Johnson, Kuppfer, and others. In
discussing the results it is convenient to compare the values (S)
found with the values (S,) calculated on tho assumption that the
volume of the alloy is equal to the sum of the volumes of the com-
ponents. Let p„ »2, P3.., stand for the relative weights of tho com-
ponents, P for their joint weight, S„Sj,S,.,.for their spocific
gravities, and we have
Separate Metals.
Copper. 25-30 I „„
Tla IcM than 7 K'™
Oopper..
.where the expression on the right hand obviously moan£ the con-
joint volume Vj of the components ; but the actual volume of the
alloy formed by their union is, in general, V- V(,(l-(-c), where «
means the expansion (or, when negative, the contraction) of unit-
volume of mixture. Hence the real valuo
S=S»/(l-^0,
«=(So-S)/S.
Matthiesen's investigation {Pogg. AnnaUnlot 1850, vol. ex. p. 21)
extends over a largo numlicr of binary alloys derived from the metak
named in the following table. Ho naturally began by procuring
pure specimens of these metals and determining their specific
^avities.
The results (each the mean of a num
as follows :—
ber of determina-
Num.
Specific
Gravity S
alCC.
(
Adopted
AtonHc
Weight.
Aiitunony.
C-7I3
7-294
SCiS
9-823
10 468
11-370*
13-573
13-265
14-3*
12-8
10-5
12-3
13-2
13-5
14-3
12-S
1J2-3
118
112
208
IDS
207-4
200
107
Cadmium..
Bhnmlli.,.
Silver
Lead
In these, as in all the subsequent determinations for the alloys,,
the weigliings were reduced to the vacuum, and the values for S
referred to water at 4° C. as unity. From eight metals twenty -eight
different kinds of binary alloys can be produced ; of these tv.-cuty-
eight combinations eighteen were selected; in each case the two com-
ponents were fused together in a variety of properly chosen atomic
proportions, and the specific gravities of these alloys were determined.
The net results are summarized iu the following table, which, for
each combination A, B, in the fiist tivo columns gives the com-
position in multiplies of the "atomic-weights" given in tho table
just quoted, while column 3 gives the values of c as calculated by
the w-riter from Matthiesen's numbers for S„ and S. Hence, for
example, in the accompanying entries the flist line shows that tho
union into an alloy of twice 118 parts
of tin and once 197 parts of gold in-
volves an expansion from 1 volume into
1 -004 ; the second that the union of onco
118 parts of tin with four times 197 parts
of gold involves a contraction from
1 volume into 1 - -028.
Tin arid Chid.
Sn 1 A
2 1 1
1 { 4
-i--00» !
-028 1
Antimony and Tin.
Antimony, Bismuth.
Antimony, Lead. |
Sb
Sn
e
Sb 1 Bi
e
Sb
Pb| e 1
12 to 8
4-2
1
1
1
1
1
lto2
3 to 10
20 to 100
+ -002
H--OOC
-1--003
+ -005
0
I to 12
0
1
2
3
5-25
+ -008
-f-00«
0
-I--0067
0
Tin. Cadmium.
Titi, Bismuth.
Tin, Silver. \
1 '" i C"
e
Sn
Bl
.
Sn
Ag
«
6
4
2
1
I
1 to 3
12
-(- -004
-I- -005
0
-001
22
4
3-1
1
1
1
1
1
4 to CO
0
--002
--005
--005
13
9
1!
3
2
1
1
1
4
-•002
-•006
-■008
-■013
-019
-024
-■«47
-•038
Tin, Gold.
Tin, Lead.
Cadmium, Bismuth.
Sii Au
'
Sn 1 Pb
«
Cd 1 Bl e
15-C
l-2-.'>
2
3
1
1
1
1
1
1
1
2
2
4
0
--002
-H-OO-J
-H-004
-I--003
+ 012
-015
--028
C
1
1
1
1
2-4
6
-I--003
+ -003
0
+ -0015
-1--005
-(-■004
3 1 1-se 0
Cadmium, Lead.
Cd Pb 1 <
6 - l-3e|oto-OOS5
BismuUi, Silver.
BismiUh, Gold.
Lead, Gold.
Bl
Ab
.
Bl
An
.
Pb
Au
«
200-2
1
1
1
4
Oto
-^■ofl2
-003
--000
-007
90
40
20
8
2
1
1
2
0
0
-003
--009
--0I7
-■035
-089
--020
10
1
1
1-
1
1
1
2
4
--0O4
-•009
-•008
-•con
-•016
-018
-004
-•Oil
METALS
69
Sismulh, I^ttd.
Lead, Silver.
Gold, Silver. ]
Bl
pb ) ;
Pb
ak
'
Au
As
«
60-JO
16
11
6
4
3
1
1
1
\
1
1
3
3
4
6
12
50
0
-•003
-■005
-■007
-CM
-■024
-■040
-■031
-•020
-015
-■010
-004
0
1
1
1
3
4
10
25
4
2
1
I
1
1
-■005
-■003
0
+■003
■f-ooe
+ ■004
+ 002
1
1
1
1
2
4
6
6
4
2
1
1
1
1
-004
-■004
-■004
— •002
-■0025
-0027
-■0024
Mercury, Tin,
Mercury, Lead.
Hg
Sn
.
Hg
Pb
'
1
1
2
2
1
1
-009
-005
-007
1
1
2
2
1
1
+ 002
-■010
-016
To make these numbers trustwoithy it would bo necessary to de-
termine their probable errors ; and this Matthiesen has not done.
It would appear that any value of e from 0 to {say)± ^002 counts for
nothing, and anything up to '004 certainly must be taken as not
proving much either way. If this is correct, then
(1) No contraction or expansion is proved in the cases Sb, Bi;
Cd, Bi i Cd, Pb ; Au, Ag ;
(2) A contraction (from O'S to 47 per cent) is proved for
Sn, Ag; Bi, Ag ; Bi.Au; Pb, Au; Pb, Bi; Hg, Sn; Hg, Pb;
Sn, Bi(?); Au, Ag (?);
(3) An expansion (from ■S to O^S percent) is proved for Sb, Sn;
Sb, Pb ; Sn, Cd (?); Sn, Pb (?); certain cases of Sn, Au aod Pb, Ag ;
(4) In the two series Sn, Au and Pb, Ag, there are cases both of
expansion and of contraction.
Thermic and Electric Properties. — The specific heat of an alloy, so
far as we know, is always in approximate accordance with Xhilong
and Pctit's law. Thus the specific heat of CujAli is
(5+1) X 6^4
6X(i3^6+lx27 '
with about the same degree of coiTectncss as the " constant" 6 '4
can claim for itself.
Expansion. — Matthiesen, from numerous determinations made
with alloys and their components, concludes that the expansion of
an alloy (from 0° to 100° C.) is nearly equal to the sum of the ex-
pansions of its components. Supposing, for instance, one volume of
gold to expand (from 0° to t) by ct, and one volume of silver by $;
■then an alloy of four volumes of gold and three volumes of silver
expands by (4a + 30)/7 per unit
Fusibility. — In the case of an alloy the melting-point and the
freezing-point are, in general, separated by a greater or less interval
of temperature, and the latter in itself may have two values as shown
by Rudbcrg, who found that when a fused alloy of tin and lead is
allowed to freeze the thermometer becomes stationai-y at two suc-
cessive points, as shown in the following table, where x means the
number of atomic weights of tin united with y of lead in the given
case, and the temperatures are in centigrade degrees.
340* isr 187' 210* (228')
1S7' isr isr isr (22s*)
We see that the first point varies with, while the second, within
the range of the experiments, proved Independent of, the proportion
in which the two metals are united.
The melting-point of many alloys lies below that of even the most
fasible component, as illustrated in the following tables, where the
numbers mean parts by weight.
Tin and Lead {Rudbcrg).
Per cent, of Tm.
Ptr cent, of Lead.
Melting point
100
0
228"
100
836
T4
26
IM
63
37
1S6
53
47
36
64
241
18
84
289
Name
of Alloy.
Tm.
lead.
Bltmotb.
Cadmlnm.
Melting-
point.
Newton's.. -.-.-.«.„
Erman's „i „.„.«.
Woods _
(Cadmium) ■
3
3
1
2
0
2
S
1
4
0
6
8
3
7
0
0
0
0
1
I
100-
95
93 7
70
(320)
All these alloys melt in boiling water.
The electric conductivity of alloys qiM alloys has been investi-
gated by Matthiesen. He confined himself to binary alloys derived
bom a certain set of elemeutaiy metals. The main results of his
researches are given in Electkioitt, vol viii. p. 61. For :iiu
practical electrician it is important to observe how very much tiit
conductivity of copper is impaired by very minute admixtures even
of metals that are good conductors, and also by non.metallic con-
tamination, especially with o.\ygen (present as CuoO).
Metallic Substances Produced by the Union, of MetaU wih
Small Proportions of Non-Metallic Elements.
Hydrogen, as vpas shown by Graham, is capable of
uniting with (always very large proportions of) certain
metals, notably mth palladium, into metal-like compounds.
But those hydrogen alloys, being devoid of metallurgic
interest, fall better under the heading Palladium.
Ox^^CTt— Mercury and copper (perhaps also other
metals) aie capable of dissolving their own oxides with
formation of alloys. Mercury, by doing so, becomes viscid
and unfit for its ordinary applications. Copper, when
pure to start with, suffers considerable deterioration in
plasticity. But the presence of moderate proportions of
cuprous oxide has been foimd to correct the evil influence
of small contaminations by arsenic, antimony, lead, and
other foreign metals. Most commercial coppers owe their
good qualities to this compensating influence.
Arsenic combines readily with all metals into tme
arsenides, which latter, in general, are soluble in the metal
itself. The presence in a metal of even small proportions
of arsenide generally leads to considerable deterioration
in mechanical qualities.
Phosphorus. — Tlie remark just made might be said to
hold for phosphorus were it not for the existence of what
is called " phosphorus-bronze," an alloy of cojjper with
phosphorus {i.e., its own phosphide), which possesses valu
able properties. According to Abel, the most favourable
effect is produced by from 1 to 1^ per cent, of phosphorus.
Such an alloy can be cast like ordinary bronze, but excek
the latter in hardness, elasticity, toughness, and tensile
strength. See Phosphorus.
Carbon. — Most metals when in a molten state are
capable of dissolving at least small proportions of carbon,
which, in general, leads to a deterioration in metallicity,
except in the case of iron, which by the addition of small
percentages of carbon gains in elasticity and tensile strength
with little loss of plasticity (see Ieon).
Silicon, so far as we know, behaves to metaLs pretty
much like carbon, but our knowledge of facts is limited.
What is known as " cast iron " is essentially an alloy of
iron proper' with 2 to 6 per cent, of carbon and more or
less of silicon (see Iron). Alloys of copper and silicon
were prepared by Deville in 1863. The alloy with 12 per
cent, of silicon is white, hard, and brittle. When diluted
down to 4 '8 per cent, it assumes the colour and fusibility
of bronze, but, unlike it, is tenacious and ductile like iron.
Action of the More Ordinary Chemical Agents on
Simple Metals.
To avoid repetition, let us state beforehand that the
metals to be referred to are always understood to be given
in the compact (frozen) conditicai, and that, wherever a
series of metals are enumerated as being similarly attacked,
the degree of readiness in the action is (so far as onr
knowledge goes) indicated by the order in which the several
members are named, — the more readily changed metal
always standing first.
Water, at ordinary or slightly elevated temperatures,
is decomposed more or less readily, with evolution of
hydrogen gas and formation of a basic hydrate, by (1)
potassium (formation of KHO), sodium (NaHO), lithium
(LiOH), barium, strontium, calcium (BaOjH^, <Jkc.) ; (2)
magnesium, zinc, manganese (MgC^Hj, <tc.).
In the case of group 1 the action is more or less violent,
and the Iiydroxides formed are soluble in water and very
70
M El A L S
strongly basylous ; mclals'of group 2 are only slowly
attacked, witli formation of relatively feebly basylous
and jiractically insoluble hydrates. Disregarding the rarer
element's (as we propose to do in this section), the metals
not named so far may be said to be proof against the
action of jmre water in the absence of free oxygen (air).
By the conjoint action of water and air, thallium, lead,
bismuth are oxidized, with formation of more or less
sparingly soluble hydrates (ThHO, PbOjH^, Bi03H3),
which, in the presence of carbonic acid, pass into still less
soluble basic carbonates.
Iron, as everybody knows, when exposed to moisture and
air, " rusts," that is, undergoes gradual conversion into a
brown ferric hydrate, Fe.fi^xHfi ; but this process never
takes place in the absence of air, and it ia questionable
whether it ever sets in in the absence of carbonic acid.
What is known is that iron never rusts in solutions of
caustic alkalies or lime (which reagents preclude the pre-
sence of free carbonic acid), while it does so readily in
ordinary moist air containing COj. When once started
the process proceeds with increasing rapidity, the ferric
hydi'ate produced acting as a carrier of oxygen; it gives
\ip part of its oxygen to the adjoining metal,, being itself
reduced to (perhaps) Fe^O^, which latter again absorbs
oxygen from the air to become ferric hydrate and so on
(Kuhlmann).
Copper, in the present connexion, is intermediate between
iron and the following group of metals.
Mercury, if pure, and all the " noble" metals (silver, gold,
platinum, and platinum-metals), are absolutely proof against
water even in the presence of oxygen and carbonic acid.
The metals grouped together above under 1 and 2 act
on steam pretty much as they do on liquid water. Of
the rest, the following are readily oxidized by steam at a
red heat, with formation of hydrogen gas, — zinc, iron,
cadmium, cobalt, nickel, tin. Bismuth is similarly attacked,
but slowly, at a white heat. Aluminium is barely affected
even at a white heat, if it is pure; the ordinary impure
metal is liable to be very readily oxidized.
Aqueous Sulphuric or Hydrochloric Acid, of course,
readily dissolves groups 1 and 2, with evolution of hydro-
gen and formation of chlorides or sulphates. The same
holds f«r the following group (A) : — [manganese, zinc,
magnesium] iron, aluminium, cobalt, nickel, cadmium.
Tin dissolves readily in strong hot hydrochloric acid as
SnCl, ; aqueous vitriol does not act on it appreciably in
the cold ; at 150° it attacks it more or less quickly, accord-
ing to the strength of the acid, with evolution of sul-
phuretted hydrogen or, when the acid is stronger, of
sulphurous acid gas and deposition of sulphur (Calvert
and Johnson). A group (B), comprising copper, are,
substantially, attacked only m the presence of oxygen or
air. Lead, in sufficiently dilute acid, or in stronger acid if
not too hot, remains unchanged. A group (C) may be
formed of mercury, silver, gold, and platinum, which arc
not touched by either aqueous acid in any circumstances.
Hot (concentrated) oil of vitriol does not attack gold,
platinum, and platinum-metals generally ; all other metals
(including even silver) are converted into sulphates, with
evolution of sulphiirous acid. In the case of iron, ferric
sijphate, Pe^(S04)3, is produced ; tin yields a somewhat
indefinite sulphate of its binoxide Sn02.
Nitric Acid- {Aqueous). — Gold, platinum, iridium, and
rhodium only are proof against the action of this powerful
oxidizer. Tin and antimony (also arsenic) are converted by
it (ultimately) into hydrates of their highest cades SnOj,
Sb^Oj (AsjOg),— the oxides of tin and antimony being
insoluble in water and in the acid itself. All other metals,
including palladium, are dissolved as nitrates, the oxidiz-
|ing part of the reagent being generally reduced to nitric
oxide, NO, or sometimes to K^Oj or N^O^. Iron, zinc,
cadmium, also tin under certain conditions, reduce the
dilute acid, partially at least, to nitrous oxide, NjO, or
nitrate of ammonia, NHj.N03 = N20 -)- 2H2O.
Aqua Beyia, a mixture of nitric and hydrochloric acids,
converts all metals (even gold, the " king of metals," whenea
the name) into chlorides, except only rhodium, iridium,
and ruthenium, which, when pure, are not attacked.
Caustic Alkalies. — Of metals not decomposing liquid
pure water, only a few dissolve in aqueous caustic
potash or soda, with evolution of hydrogen. The most
irnportant of these are aluminium and zinc, which are
converted into alumiuate, AL,033(K2 or Na,)0, and
zincate, ZnO.RHO, where R^K or' Na respectively.
But of the rest the majority, when treated with boiling
sufficiently strong alkali, are attacked at least superficially;
of ordinary metals ordy gold, platinum, and silver are
perfectly proof against the reagents under consideratioi^
and these accordingly are used preferably for the construc-
tion of vessels intended for analytical operations involving
the use of aqueous caustic alkalies. For preparative
purposes iron is universally employed and works well ; but
it is not available analytically, because. a superficial oxida-
tion of the empty part of the vessel (by the water and air)
cannot be prevented. According to the writer's experience
basins made of pure malleable nickel are free from this
drawback ; they work as well as platinum, and rather better
than silver ones do. There is hardly a single metal which
holds out against the alkalies themselves when in the state
of fiery fusion ; even platinum is most violently attacked.
In chemical laboratories fusions with caustic alkalies are
always effected in vessels made of gold or silver, these
metals holding out fairly well even in the presence of air.
Gold is the better of the two. Iron, which stands so well
against aqueous alkalies, is most violently attacked by the
fused reagents. Yet tons of caustic soda are fused daily
in chemical works in iron pots without thereby suffering
contamination, which seems to show that (clean) iron,
like gold and silver, is attacked only by the conjoint
action of fused alkali and air, the influence of the latter
being of course minimized in large-scale operatioris.
Oxygen or Air. — The noble metals (from silver upwards)
do not combine directly with oxygen given as oxygen gas
(Go), although, like silver, they may absorb this gas largely
when in the fused condition, and may not be procr against
ozone, Oy Mercury, within a certain range of tempera-
tures situated close to its boiling point, combines slowly
with oxygen into the red oxide, which, however, breaks up
again at higher temperatures. All other metals, when
heated in oxygen or air, are converted, more or less readily,
into stable oxides. Potassium, for example, yields peroxide,
K0O2 or KjOj ; sodium gives NajO,, ; the barium-grouii
metals, as well as magnesium, cadmium, zinc, lead, copper,
are converted into their monoxides MeO. Bismuth and
antimony give (the latter very readily) sesquioxide (Bi.,Oj
and SbjOg, the latter • being capable of passing into
Sb.,04). Aluminium, when pure and kept out of contact
with siliceous matter, is only oxidized at a white heat,
and then very slowly, into alumina, AUOj. Tin, at high
temperatures, passes slowly into binoxide, SnOj.
Sulphur. — Amongst the better known metals, gold and
aluminium are the only ones which, when heated with
sulphur or in sulphur vapour, remain unchanged. All the
rest, under these circumstances, are converted into sulphides.
The metals of the alkalies and nlkaliao earths, also
magnesium, bum in sulphur-vapour as they do in oxygen.
Of the heavy meals, copper is Uio one which exhibits by
far the greatest avidity for sulphur, its subsulphide Cu^S_
being the stablest of all hea^-y metallic sulpliides m
opposition to dry reactions. Sec MjETAtLtniGY.
M E T — M E T
71
Chionn^.-^AU metals, when treated with chlorine gas at
the proper temperatures, pass into chlorides. In some
cases the chlorine is taken up in two instalments, a lower
chloride being produced first, to pass ultimately into a
higher chloride. Iron, for instance, is converted first
into FeClj, ultimately into FejCl^, which practically means
a mixture of the two chlorides, or pure FcjCl. as a final
product. Of the several products, the chlorides of gold
and platinum (AUCI3 and PtCl,) are the only ones which
when heated beyond their temperature of formation
dissociate into metal and chlorine. The ultimate chlorina-
tion product of copper, CuClj, when heated to redness,
decomposes into the lower chloride, CUjClj, and chlorine.
All the rest, when heated by themselves, volatilize, some
at lower, others at higher temperatures.
Of the several individual chlorides, the following are
liquids or solids, volatile enough to be distilled from out
Of glass vessels :— AsClj, SbClj, SnCl^, BiClj, HgCl^ the
'chlorides of arsenic, antimony, tin, bismuth, mercury re-
spectively. The following are readily volatilized in a
Current of chlorine, at a red heat : — AljClj, OjClj, FCjClu,
the chlorides of aluminium, chromium, iron. The follow-
ing, though volatile at higher temperatures, are not vola-
tilized at dull redness :— KCl, NaCl, LiCl, NiClj, CoClj,
MnCl^ ZnClj, MgClj, PbClj, AgCl, the chlorides of
I>ot;issium, sodium, lithium, nickel, cobalt, manganese,
zinc, magnesium, lead, silver. Somewhat less volatile
than the last named group are the chlorides (MClj) of
barium, strontium, and calcium.
Metallic chlorides, as a class, are readily soluble in
■niter. The following are the most important exceptions ^
— chloride of silver, AgCl, and subchloride of mercury,
E^oCl^ are absolutely insoluble ; chloride of lead, PbC'lj,
and subchloride of copper, Cu^CIj, are very sparingly
soluble in water. The chlorides AsClj, SbClj, BiClj, are at
once decomposed by (liquid) water, with formation of
oxide (AsjOj) or oxychlorides (SbClO, BiClO) and hydro-
chloric acid. The chlorides MgCl.^ AIjCl^ Cr.^Clp Fe^Clj
suffer a similar decomposition when evaporated with water
in the heat. The same holds in a limited sense for ZnCL^,
CoCl ,, NiCL, and even CaCl^. All chlorides, except those
of silver and mercury (and, of course, those of gold and
platinum), are oxidized by steam at high temperatures,
wth elimination of hydrochfcric acid.
The above statements concerning the volatilities and
solubilities of metallic chlorides form the basis of a
number of important analytical methods {or the separation
of the respective metals.
'For the characters of metals as cnemical elements the
reader is referred to t"he article Chemistey and to the
special articles on the different mefals. (w. D.)
ilETAL-WORK. Among the many stages in the- de-
velopment of primeval man, none can have been of greater
moment in his struggle for existence than the discovery
of the metals, and the means of working them. The
Jiames generally given to the three prehistoric periods of
man's life on the earth — the Stone, the Bronze, and the Iron
age — imply the vast importance of the progressive steps
from the flint knife to the bronze celt, and lastly to the
keen-edged elastic iron weapon or tool. The length of
time during which each of these ages lasted must of course
have been different in every country and race in the world.
The Digger Indians of South California have even now
not progressed beyond the Stone Age ; while some of the
tribes of Central Africa are acquainted with the use of
copper and bronze, though they are unable to_6melt ot
work iron.
\he metals chiefly used have oeen gold, silver, copper
ai\d^in (the last two generally mixed, forming an alloy
called bronze), iron, and lead. » The peculiarities of these
various metals havrnaturally marked out each of them for*
special uses and methods of treatment. The durability and
the extraordinary ductility and pliancy of gold, its power of
being subdivided, drawnr out, or flattened into wire or leaf
of almost infinite fineness, have led to its being used for
works where great minuteness and delicacy of execution
were required ; while its beauty and rarity have, for the
most part, limited its use to objects of adornment and
luxury, as distinct from those of utility. In a leaser
degree most of the qualities of gold are shared by silver,
and consequently the treatment of these two metals has
always been very similar, though the greater abundance
of the latter metal has allowed it to be used on a larger
scale and for a greater variety of purposes.
Bronze is an alloy of copper and tin in varying propoP
tions, the proportion of tin being from 8 to 20 per cent'
The great fluidity of bronze when melted, the slightness 6f
its contraction on solidifying, together with its density and
hardness, make it especially suitable for casting, and alloit'
of its taking the impress of the mould with extreme sharp^
ness and delicacy. In the form of plate it can be tempered
and annealed till its elasticity and toughness are much
increased, and it can then be formed into almost any shapA
under the hammer and punch. By other methods of
treatment, known to the ancient Egyptians, Greeks, and
others, but now forgotten, it could be hardened and formed
into knife and razor edges of the utmost keenness. In
many specimens of ancient bronze small quantities of
silver, lead, and zinc have been found, but their presence
is probably accidental.
In modem times, after the discovery of zinc, an alloy of
copper and zinc called brass has been much used, chiefly
for the sake of its cheapness as compared vrith bronze. In'
beauty, durabihty, and delicacy of surface it is very inferior
to bronze, and, though of some commercial importance, has
been of but little use in the production of works of art.
To some extent copper was used in an almost pure state
during mediaeval times; especially from the 12th to the
15th century, mainly for objects of ecclesiastical use, suclr
as pyxes, monstrances, reliquaries, and croziers, partly oi)
account of its softness under the tool, and also because if
was slightly easier to apply enamel and gilding to pure
copper than to bronze (see fig. 1). In the mediaeval
period it was used to some extent in the shape of thin
sheeting for roofs, as at St Mark's, Venice ; while during
the 16th and 17th centuries it was largely employed for
ornamental domestic vessels of various sorts.
Iron} — The abundance in which iron is found in so
many places, its great strength, its remarkable ductilit^
and malleability in a red-hot state, and the ease with;
which two heated surfaces of iron can be welded together
under the hammer combine to make it specially suitable
for works on a large scale where strength with lightness
are required — things such as screens, window-grills, oma-_
mental hinges, and th« like.
In its hot plastic state iron can be formed and modelled
under the hammer to almost any degree of refinement,
while its great strength allows it to be beaten out into
leaves and ornaments of almost paper-like thinness and
delicacy. With repeated hammering, drawing out, and
annealing, it gains much in strength and toughness, &nd
the addition of a very minute quantity of carbon converts'
' Some recent analyses of the iron of prehistoric weajjons have
brought to light the interesting fact that many of these earlieat
specimens of iron manufacture contain a considerable percentage of
nickeL Tliis special alloy does not occur in any known iron ores^
but is invariably found in meteoric iron. It thus appears that iron
was manufactured from meteorolites which had fallen to the earth in
an almost pure metallic state, possibly long before prehistoric man
had learnt bow to dig for and smelt iron in any of the forma of ore
which are found oil this planet.
72
METAL- AV OEK
it into feteel, less tough, but of the keenest hardness." The
iarge emijloyment of cast iron is comparatively modern, in
England at least only dating from the 16th century; it is
not, however, incapable of artistic treatment if due regard
be paid to the necessities of casting, and if no attempt is
made to imitate the fine-drawn lightness to which wrought
iron so readily lends itself. At the best, however, it is not
generally suited for the finest work, as the great contrac-
tion of iron in passing from the fluid to the solid state
renders the cast somewhat blunt and spiritless.
Among the Assyrians, Egyptians, and Creeks the use of
iron, either cast or wrought, was very limited, bronze being
the favourite mfetal for
almost all purposes.
The difiiculty of smelt-'
ing the ore was prob-,
ably one reason for
this, as well as thd
now forgotten skilli
which enabled bronzffi
to be tempered to a
steel-like edge. Ithad,
however, its value, of
which a proof occurs'
in Homer (II. xxiii.),
where a mass of iron
is mentioned as being
one of the prizes at
the funeral games of
Patroclus.
Methods of Manipu-
lation in Metal- Work.
— Gold, silver, and
bronze may be treated
in various ways, the'
chief of which are (1)
casting in a mould,
and (2) treattoent by
hammeringand punch-
ing (French, repousse).
, The first of these,
casting, is chiefly
adapted for bronze,
or in the case of the
more precious metals
only if they are used
on a very small scale.
The reason of this is
that a repouss6 relief
is of much thinned
substance than if the
same design were cast,
even by the most
skilful metal-worker,
and so a largo surface
may be produced with
a very small expendi-
ture of valuable metitl.
Casting is probably
the most primitive
metliodof metal-work.
This has passed tlu-ough three stages, the fu-st being
Tepresented by solid casting-s, such' as are most celts and
tither implements of the prehistoric time ; the mould
'vaa formed of clay, sand, or stone, and the fluid metal
was poured in tdl the hoUow w^s full. The next stage
waa, in the case of bronze, to introduce an iron core, prob-
ably to save needles-s ox])endituro of tho more valuable
metal. The British Museum possesses an interesting
iEtrascan or Arclmic Italiau example of this primitive
device. It is'a bronze statuette from Sessa on the Voltumo,
about 2 feet high, of a female standing, robed in a close-
fitting chiton. The presence of the iron core has been
made visible by the splitting of the figure, owing to the
unequal contraction of the two metals. The forearms,
which are extended, have been cast separately and soldered
or brazed on to the elbows.
The third and last stage in the progress ol tho art of
casting was the employment of a core, generally of clay,
round which tho metal was cast in a mere skin, only thick
enough for strength, without waste of metal. The Greeks
and Komans attained to the greatest possible skill in this
process. Their exact method is not certainly known,
but it appears probable that they were acquainted with
the process now called ci cire perdue — the same as that
employed by the great Italian artists in bronze, and
still unimproved upon even at the present day. Cellini,
the great Florentine, artist of the 16th century, has
described it fully in his Trattato delta Sculiura. If a
statue was to be cast, the figure was first roughly modelled
in clay — only rather smaller in all its dimensions than the
future bronze ; all over thb a skin of wax was laid, and
worked by the sculptor with modelling tools to the required
form and finish. A mixture of pounded brick, clay, and
ashes was then ground finely in water to the consistence of
cream, and successive coats of this mixture were then
applied with a brush, till a second skin was formed all
over the wax, fitting closely int^ every line and depression
of the modelling. Soft clay was then carefully laid on to
sttengthen the mould, in considerable thickness, till the
whole statue appeared like a shapeless mass of clay, round
which iron hoops were bound to hold it all together. Tue
whole was then thoroughly dried, and placed in a hot (jven,
which baked the clay, both of the core and the outside
mould, and melted the wax, which was allowed to run out
from small holes liiade for .the purpose. Thus a hollow
was left, corresponding to the skin of wax between the core
and the mould, the relative positions of which were pre-
served by various small rods of bronze, which had pre-
viously been driven through from the outer mould to the
rough core. The mould was now ready, and melted bronze
was poured in till the whole space between the core and
the outer mould was full After slowly cooling, the outer
mould was broken away from outside the statue, and tha
inner core as much as possible broken up and raked out
through a hole in the foot or some other part of the statue.
The projecting rods of bronze were then cut away, and
the whole finished by rubbing down and polishing over any
roughnesses or defective places. The most skilful sculptors,
however, had but little of this after-touching to do, the
final modelling and even poHsh which they had put upon
the was being faithfully reproduced in the bronze casting.
The further enrichment of the object by enamels and
inlay of other metals was practised at a very early period
by Assyrian, Egyptian, and Greek metal-workers, as weD
as by the artists of Persia and mediieval Europe.
The second chief process, that of hammered work (Greek,
sphyrelata ; French, repousse), was probably adopted for
bronze-work on a large scale, before the art of forming
large castings was discovered. In the most primitive
method thin plates of bronze were hammered over a
wooden core, rudely cut into the required shape, the core
serving the double purpose of giving shape to and
strengthening the thin metal.
A further development in the art of hammered woit
consisted in laj-ing the metal plate on a soft and elastic
bed of cement made of pitch and pounded brick. The
design was then beaten into relief from the back with
hammers and jiunches, tho pitdi bed yielding to the
protuberanoce which were thus formed, and serving to prf^
METAL- WORK
rs
Vent the punch from breaking the metal into holes. The
pitch was then melted away from the front of the embossed
relief, and applied in a similar way to the back, so that the
modelling could be completed on the face of the relief,
the final touches being given by the graver. This process
was chiefly applied by mediaeval artists to the precious
metals, but by the Assyrians, Greeks, and other early
nations it was largely used for bronze.
The great gates of Shalmaneser 11., 859-824 B.C., from
Balawat, now in the British Museum, are a remarkable
example of this sort of work on a large scale, though the
treatment of the reliefs is minute and delicate. The " Siris
bronzes," in the same museum, are a most astonishing
example of the skill attained by Greek artists in this
reponss^ work (see Bronsted's Bronsts of Siris, 1836).
They are a pair of shoulder-pieces from a suit of bronze
armour, and each has m very high relief a combat between
a Greek warrior and an Amazon. No work of art in
metal has probably ever surpassed these little figures for
beauty, vigour, and expression, while the skill with which
the artist has beaten these high reliefs out of a flat plate
of metal appears almost miraculous. The heads of the
figures are nearly detached from the ground, their sub-
stance is little thicker than paper, and yet in no place
has the metal been broken through by the puncL They
are probably of the school of Praxiteles, and date from the
<th centtiry Bx;. (see fig. 2).
/ Fia 2.— One o( the Siiis Bronzes.
Copper and tin have been but little used separately.
Copper in its pure state may be worked by the same
Ibethods as bronze, but it is inferior to it in Lardness,
strength, and beauty of surface. Tin is too geak and
brittle a metal to be employed alone for any but email
objects. Some considerable number of tin drinking-cups
and bowls of the Celtic period have been found in Corn-
wall in the neighbourhood of the celebrated tin and copper
mines, which appear to have been worked from a very early
period. The existence of these mines was known to the
Phoenicians, who carried on a considerable trade in metals
with the south-west comer of England and the Scilly Isles
— probably the Cassiterides of Pliny and other classical
writers.
The use of lead has been more extended. In sheets it
forms the best of all coverings for roofs and even spires.
In the Roman and mediaeval periods it was largely used
for cofiins, which were often richly ornamented with cast
work in relief. Though fusible at a very low temperature,
and very soft, it has great power of resisting decay from
damp or exposura Its most important use in an artistic
form has been in the shape of baptismal fonts, chiefly
between the 11th and the 14th centuries. The superior
beauty of colour and durability of old specimens of lead is
owing to the natural presence of a small proportion of
silver. Modem smelters carefully extract this silver from
the lead ore, thereby greatly impairing the durability and
beauty of the metal
As in almost all the arts, the ancient Egyptians excelled
in their metal-work, especially in the use of bronze and
the precious metals. These were worked by casting and
hammering, and ornamented by inlay, gilding, and enamels
with the greatest possible skill.
From Egypt perhaps was derived the early skill of t&
Hebrews. Further instruction in the art of metal-working
came probably to the Jews from the neighbouring country
of Tyre. The description of the great gold lions of
Solomon's throne, and the laver of cast bronze supported
on figiires of oxen, shows that the artificers of that time had
overcome the difficulties of metal-working and founding
on a large scale. The Assyrians were perhaps the most
remarkable of all ancient nations for the colossal size and
splendour of their works in metal j whole circuit walls of
great cities, such as Ecbatana, are said to have been
covered with metal plates, gilt or silvered.
Herodotus, Athenaeus, and other Greek and Koman
writers have recorded the enormous number of colossal
statues and other works of art for which Babylon and
Nineveh were so famed. The numerous objects of bronze
and other metals brought to light by the excavations of
the last forty years in the Tigris and Euphrates valleys,'
though mostly on a small scale, bear witness to the great
skill and artistic power of the people who produced them;
while the recent discovery of some bronze statuettes,
shown by inscriptions on theln to be not later than 2200
B.O., proves how early was the development of this branch
of art among the people of Assyria.
The Metal- Work of Greece. — The poems of Homer are
full of descriptions of elaborate works in bronze, iron, gold,
and silver, which, even when fulf allowance is made for
poetic fancy, show clearly enough a very advanced amount
of skill in the working and ornamenting of these metals
among the Greeks of his time. His description of the
shield of Achilles, made of bronze, enriched with bands of
figure reliefs in gold, silver, and tin, cotdd hardly have
been written by a man who had not some personal
acqtiaintance with works in metal of a very elaborate kind.
Again, the accuracy of his descriptions of brazen houses —
such as that of Alcinous, Od. vii. 81 — is borne witness to by
Pausanias's mention of the bronze temple of Athen*
XoAkiouco? in Sparta, and the bronze chamber dedicated
to Myron in 648 B.C., as well as by the discovery of die
stains and bronze nails, which show that the whole interior
of the so-called treasury of Atreus at Mycen« was once
T4
M E T A L-W 0 R K
oorered ■with a lining of bronze plates. Of the two chief
methods of working bronze, gold, and silver, it is probable
that the hammer process was first practised, at least for
statues, among the Greeks, who themselves attributed the
invention of the art of hollow casting to Theodorus and
Ehoecus, both Samian sculptors, about the middle of the
6th century B.a Pausanias spicially mentions that ono
of the oldest statues he had ever seen was a large figure
of Zeus in Sparta, made of hammered bronze plates riveted
together. With increased skill in large castings, and the
discovery of the use of cores, by which the fluid bronze
was poured into a mere skin-like cavity, hammered or
repouss^ work (Greek, sphyrdata) was only used for small
objects where lightness was desirable, or for the precious
metals in order to avoid large expenditure of metsi The
colossal statues of ivory and gold by Phidias were the
most notable examples of this use of gold, especially his
statue of Athena in the Parthenon, and the one of Zeus at
Olympia. The nude parts, such as face and hands, were
of ivory, while the armour and drapery were of beaten
gold. The comparatively small weight of gold used by
Phidias is very remarkable when the great size of the
statues is considered.
A graphic representation of the workshop of a Greek
sculptor in bronze is given on a fictile vase now in the
Berlin Museum ^see Gerhard's TrinkschaZen, plates xii.,
sdii.). One man is raking out the fire in a high furnace,
while another behind is blowing the bellows. Two others
are smoothing the surface of a statue with scraping tools,
formed like a strigiL A fourth is beating the arm of an
unfinished figure, the head of which lies at the workman's
feet. Pemaps ihe most important of early Greek works in
cast bronze, both from its size and great hLstorical interest,
is the bronze pillar (now in the Hippodrome at Constanti-
nople) which was erected to commemorate the victory of
the allied Greek states over the Persians at Plataea in 479
B.C. (see Newton's Travels in the Levant). It is in the form
of three serpents twisted together, and before the heads
were broken off was at least 20 feet high. It is cast
hollow, all in one piece, and has the names of the allied
states engraved on the lower part of the coils. Its size
and the beauty of its surface show great technical sldll in
the founder's art. On it once stood the gold tripod dedi-
cated to ApoUo as a tenth of the spoils. It is described
both by Herodotus and Pausanias.
Marble was comparatively but little used by the earlier
Greek sculptors, and even Myron, a rather older man than
Phidias, seems to have executed nearly all his most im-
portant statues in metaL
. Additional richness was given to Greek bronze-work by
-old or silver inlay on hps, eyes, and borders of the dress ;
one remarkable statuette in the British Museum has eyes
inlaid with diamonds, and fret-work inlay in silver on the
border of the chiton.
The mirrors of the Greeks are among the most important
specimens of their anistio metal-work. These are bronze
disks, one side polished to serve as a reflector, and the back
ornamented with engraved outline drawings, often of great
beauty (see Gerhard, Etrmkisdie Spiegel, 1843-67).
The Greek workman, in fact, was incapable of making
an ugly thing. Whatever the metal or whatever the object
formed, whether armour, personal ornaments, or domestic
vessels, the form was always specially adapted to its use,
the ornament natural and graceful, so that the commonest
water-jar was a delight alike to him who made it and those
who used it.
In metal-work, as in other arts, the Romans were pupils
and imitators of the Greeks. 0\nng to the growth of that
spirit of luxury which in time caused the extinction of the
fioman empire, a considerable demand arose for magni-
ficent articles of gold and silver plate. The finest Bpcii-
mens of these that still exist are the very beautiful set of
silver plate found buried near Hildcsheim in 1869, now in
the Berlin Museum. Thay consist of drinking vessels,
bowls, vases, ladles, and other objects of siKer, parcel-gilt,
and exquisitely decorated with figures in relief, both cast
and repouss^. There are electrotyjjes of these in the
South Kensington Museum.
When the seat of the empire was changed from Borne
to Byzantium, the latter city became the chief centre for
the production of artistic metal-work. From Byzantium
the special skill in this art -was transmitted in the 9th and
10th centuries to the Rhenish provinces of Germany and
to Italy, and thence to the whole of Western Europe ; in
this way the 18th-century smith who wrought the Hamp-
ton Court iron gates was the heir to the mechanical skill'
of the ancient metal-workers of Phoenicia and Greece.
In that period of extreme degradation into which all the
higher arts fell after the destruction of the Roman empire,
though true feeling for beauty and knowledge of the
subtleties of the human form remained for centuries almost
dormant, yet at Byzantium at least there still survived
great technical skill and power in the production of all
sorts of metal-work. In the age of Justinian (first half
of the 6th century) the great church of St Sophia at
Constantinople was adorned with an almost incredible
amount of wealth and splendour in the form of screens,
altars, candlesticks, and other ecclesiastical furniture made-
of massive gold and silver.
Metal-Work in Italy.— It was therefore to Byzantium
that Italy turned for metal-workers, and especially for gold-
smiths, when, in the 6th to the 8th centuries, the basilica
of St Peter's in Rome was enriched with masses of gold
and silver for decorations and fittings, the gifts of many
donors from Belisarius to Leo HL, the mere catalogue of
which reads like a tale from the Arabian Nights. The
gorgeous Pala d'Oro, still in St Mark's at Venice, a_gold
retable covered with delicate reliefs and enriched with
enamels and jewels, was the work of Byzantine artists
during the 11th century. This work was in progress for
more than a hundred years, and was set in its place in
1106 A.D., though still unfinished (see Bellomo, Pala d'Oro
di S. Mareo, 1847).
It was, however, especially for the production of bronze
doors for churches, ornamented with panels of cast work
in high relief, that Italy obtained the services of Byzantine
workmen (see Garrucci, Arte Cristiana, 1-872-82). One
artist named Staurachios produced many works of this
class, some of which stQl exist, such as the bronze doors
of the cathedral at Amalfi, dated 1066 A.D. Probably
by the same artist, though his name was spelled dif-
ferently, were the bronze doors of San Paolo fuori le
Mura, Rome, careful di-awings of which exist, though the
originals were destroyed in the fire of 1824. Other
important examples exist at Ravello (1197), Salerno
(1099), iVmalfi (1062), Atrani (1087) ; and doors at Mon-'
realo i» Sicily and at Trani, signed by an ai-tist named
Barisanos (end of the 12th century); the reliefs on these
last are remarkable for "expression and dignity, in spite
of their early rudeness of modelling and ignoitince of the
human figure.
Most of these works in bronze were enriched with fine'
lines inlaid in silver, and in some cases with a kind of
niello or enamel. The technical skill of these Byzantine
roetal-'workers was soon acquired by native Italian artists,
wfio produced many important works in bronze similar in
style and execution to those of tlio Byzantine Greeks.
Such, for example, are the bronze doors of San Zenone at
'Verona (unlike the others, of repous.si; not cast work) ; those
C'f the Duomo of Pisa, cast in 1 ISO by Bonanmis, and of the
M E T A L-W 0 R K
75
Dnomo of Troia, the last made in the beginning of the 12th
oentoiy by Oderisiua of Benevento. Another artist named
Roger of Amnlfi worked in the same way; and in the
year 1219 the brothers Hubertos and Fetrus of Piacenza
cast the bronze door for one of the side chapels in San
Qiovanni in Laterano. One of the most important early
roecimens of metal-work b the gold and silver altar of
mnf Ambrogio in Hilan. In character of work and
desiga it resembles the Yenice Fala d'Oro, but is still
earlier in date, being a gift to the church from Arch-
bishop Angilbert IL in 835 A.D. (see Du Sommerard,
and D'Aginconrt, Itoyen Age). It is signed wolvinivs
HAOISTEB PHASES ; nothing is known of the artist, but he
probably belonged to the semi-£yzantine school of the
Rhine provinces ; according to Dr Bock he was an Anglo-
Saxon goldsmith. It is a very sumptuous work, the front
of the altar being entirely of gold, with repouss^ reliefs
and cloisonne enamels ; the back and ends are of silver,
with gold ornaments. On the front are figures of Christ
and the twelves apostles ; the ends and back have reliefs
illustrating the life of St Ambrose.
The most important existing work of art in metal of the
13th century is the great candelabrum now in Milan
cathedral It \s of gilt bronze, more than H feet high;
it has seven branches for candles, and its upright stem
is supported on four winged dragons. For delicate and
spirited execution, together with refined gracefulness of
design, it is uns'urpassed by any similar work of art. Every
one of the numerous little figures with which it is adorned
is worthy of study for the beauty and expression of the face,
and the dignified arrangement of the drapery (see fig. 3).
Flo. 8. — Boss from the Mibne.<ie Candelabmm.
ITie semi-conventional open scroll-work of branches and
fruit which wind around and frame each figure or group is
devised with the most perfect taste and richness of fancy,
while each minute part of this great piece of metal-work
is finished with all the care that could have been bestowed
on the smallest article of gold jewellery. Though some-
thing in the grotesque dragons of the base recalls the
Byzantine sqhool, yet the beauty of the figures and the
keen feeling for graceful curves and folds in the drapery
point to a native Italian as-being the artist who produced
this wonderful work of art. There is a cast in the South
Kensington Museum.
During the 13th and 14th centuries in Italy the wide-
spread influence of Niccolo Fisano and his school encouraged
the spulptor to use marble rather than bronze for his work.
At this period wrought iron came into general use in the
form of screens for chapels and tombs, and grills for
windows. These are mostly of great beauty, and show
itmarkable-skill in the use of the hammer, as well as power
in adapting the design to the requirements of the material
Among the finest examples of this sort of work are the
screens round the tombs of the Scala family at Verona,
1350-75, — a sort of net-work of light cusped quatrefoils,-
each filled up with a small ladder (scala) in allusion to
the name of the family. The most elaborate specimen of
this wrought work is the screen to the Rinuocini chapel in
Santa Croce, Florence, of 1371, in which moulded pillars
and window-like tracery have been wrought and modelled
by the hammer with extraordinary skill (see Wyatt, Metal-
Work of Middle Ages). Of about the same date are the
almost equally magnificent screens in Sta Trinita, Florence,
and at Sien^ across the chapel in the Palazzo Pubblica
The main part of most of these screens is filled in with
quatre-foils, and at the top is an open frieze formed of
plate iron pierced, repouss^ and enriched with engraving.
In the 14th century great quantities of objects for
ecclesiastical use were produced in Italy, some on a large
scale, and mostly the works of the best artists of the time.
Fia 4. — Silver Repousse' Reliefs from the Pistoia Retable.
The silver altar of the Florence baptistery is one of the
chief of these; it was begun in the first half of the 14th
century, and not completed till after 1477 (see Gaz. dee
Beaux Arts, Jan. 1883). A whole series of the greatest
artists in metal laboured on it in succession, among whom
were Orcagna, Ghiberti, Verrocchio, Ant. Pollajuolo, and
many others. It has elaborate reliefs in repouss^ work, cast
canopies, and minute statuettes, with the further enrich-
ment of translucent coloured enamels. The silver altar
and retable of Pistoia cathedral (see fig. 4), and the great
shrine at Orvieto, are works of the same class, and of equal
importance.
Whole volumes might be devoted to the magnificent
works in bronze produced by the Florentine artists of this
century, works such as the baptistery gates by Ghiberti,'
and the statues of Verrocchio, Donatello, and^HRDy
others, but these come rather under the bead of sculpture.-
76
METAL- WORK
Some very magnificent bronze screens were produced at
this time, especially that in Prato cathedral by Simone,
brother of DonatcUo, in 1444^01, and the screen and bronze
ornaments of the tomb of Piero and Giovanni dei Medici
in San Lorenzo, Florence, by Verrocchio, in 1472.
At the latter part of the 15th century and the beginning
of the 16th the PoUajuoli, Ricci, and other artists devoted
much labour and artistic skill to the production of candle-
sticks and smaller objects of bronze, such as door-knockers,
many of which are works of the greatest beauty. The
candlesticks in the Certosa near Pavia, and in the cathedrals
of Venice and Padua, are the finest examples of these.
Niccolo Grossi, who worked in wrought iron under the
patronage of Lorenzo dei ^ledici, produced some wonderful
specimens of metal-work, such as the candlesticks, lanterns,
and rings fi-xed at intervals round the outside of the great
palaces (see fig. 5). The Strozzi palace in Florence and
Fia. 5.— WrougTit Iron Candle-Pricket ; late 15th-century.
Florentine T\'ork.
the Palazzo del Magnifico at Siena have fine specimens of
these, — the former of wrought iron, the latter in cast bronze.
At Venice fine work in metal, such as salvers and vases,
was being produced, of almost Oriental design, and in
some cases the work of resident Arab artificers. Li the
16th century Benvenuto Cellini was supremo for skill in
the production of enamelled jewellery, plate, and even larger
works of sculpture (see Plon's Ben. Cellini, 1882), and John
of Bologna in the latter part of the same century inherited
to some ertent the skill and artistic power of the great
15f,h-contury artists. Since that time Italy, like other
countries, has produced little metal-work of real value.
Spain. — From a very early period the metal-workers of
Spain have been distinguished for their skill, esjjceially in
the use of the precious metals. A very remarkable set of
epecimens of goldsmith's work of tlie 7th century are the
deven votive crowns, two crosses, and other objects found
in 1858 at Guarrazar, and now presen-ed at Madrid and in
Pai-is in the Cluny Museum (see Du Sommerard, Musce ck
Clnny, 1852). ilagnificent works in silver, such as shrines,
altar cros.ses, and church vessels of all kinds, were pro-
duced in Spain from the 14th to the 16th century, —
especially a number of sumptuous tabernacles (custodia)
for the host, magnificent examples of which still exiBt
in the cathedrals of Toledo and Seville. The bronae
and wrought iron screens — ryas, mostly of the 15th
and 16th centuries — to be found in almost every im-
portant church in Spain are very fine examples of metal-
work. They generally have moulded rails or ballusters,
and rich friezes of pierced and repoussd work, the whole
being often thickly plated with silver. The common use
of metal for puljiits is a peculiarity of Spain; they are
sometimes of bronze, as the pairs in Burgos and Toledo
cathedrals, or in wrought iron, like those at Zamora and
in the church of San Gil, Burgos. The great candelabrum
or ienehrarium in Seville cathedral is the finest speci-
men of 16th-cc:ntury metal-work in Spain ; it was mainly
the work of Bart. Morel in 1562. It is of cast bronze
enriched with delicate scroll-work foliage, and with num-
bers of well-modelled statuettes, the general effect being
very rich and graceful. Especially in the art of metal-
work Spain was much influenced in the 15th and 16th
centuries by both Italy and Germany, so that numberless
Spanish objects [iroduced at that time owe little or nothing
to native designers. At an earlier period Arab and Moor-
ish influence is no less apparent.
England. — In Saxon times the English metal-workers,
especially of the precious metals, possessed great skill, and
ajjpear to have produced shrines, altar-frontals, retables,
and other ecclessiastical furnituro of considerable size and
magnificence.
Dunstan, archbishop of Canterburj- (925-988), like
Bernward, bishop of Hildesheim a few years later, and St
Eloi of Franco three centuries earlier, was himself a skilful
worker in all kinds of metal. The description of the gold
and silver retable given to the high altar of Ely by Abbot
Theodwin in the 1 1th century, shows it to have been a large
and elaborate piece of work decorated with many reliefs
and figures in the round. Jn 1241 Henry TIL gave the
order for the great gold shrine to contain the bones of
Edward the Confessor (see W. Burges in Gleanings from.
Westinin.'iter). It was the work of members of the Otho
family, among whom the goldsmith's and coiner's crafts
appear to have been long hereditary. Countless other
important works in the precious metals adorned every
abbey and cathedral church in the kingdom.
In the 13th century the English workers in wrought
iron were especially skilful The grill over the tomb of
Queen Eleanor at Wc.stmiiifter, by Thomas de Lcghton,
made about 1294, is a remarkable example of skill in weld-
ing and modelling with the hainmnr (sr.i- fig. 6).
The rich and graceful iron hinges, made often for small
and out-of-the-way country churches, are a large and
important class in the list of English -nTought iron-work.
Those on the refectory door of Merton College, Oxford,, are
a beautiful and well-preserved example dating from the
14 th century.
More mechanical in execution, though still very rich in
effect, is that sort of iron tracery work produced by cutting
out patterns in plate, and superimposing one plate over
the other, so as to give richness of effect by the shadows
jiroduccd by these varjnng planes. The screen by Henry
V.'s tomb at Westminster is a good early specimen of thia
land of work.
The screen to Bishop West's chapel at Ely, and that
round Edward IV. 's U>m\i at Windsor, both made towards
the end of the 15th centurj', ore the most magnificent
M'ETAL-WORK
77
English (jxamples of wrought iron, in which every art and
feat of skill known to the smith has been brought into
play to give variety and richness to the work.
I Much WTought-iron work of great beauty was produced
at the beginrung of the 18th century, especially under the
superintendence of Sir Christopher Wren (see Ebbetts,
Iron Work of i7lh and I8(h Centuries, 1880). Large
flowing leaves of acanthus and other plants were beaten
out with wonderful spirit and beauty of curve. The
gates from Hampton Court arc the finest examples of
this class of work (see fig. 7).
From an early period broiue and latten (a variety of
brass) were much used in England for the smaller objects
both of ecclesiastical and domestic use, but except for
tombs and lecterns were but little useu on a large scale till
the 16th century. The full-length recumbent effigies of
Henry III. and Queen Eleanor at Westminster, cast in
bronze by the " cire perdue " process, and thickly gUt, are
equal, if not superior, in artistic beauty to any sculptor's
work of the same period (end of the 13th century) that was
produced in Italy or elsewhere. These effigies are th6 work
Fig. 6.— Part of the "Eleanor Grill."
of an Englishman named William Torel (see Westminster
Gleanings). The gates to Henry VII.'s chapel, and the
screen round his tomb at Westminster (see fig. 8), are very
elaborate and beautiful examples of " latten " work, show-
ing the greatest technical skiU in the founder's art. In
latten also were produced the numerous monumental
brasses of which about two thousand still exist in England.
Though a few were made in the 13th century, yet it was
not till the 14th that they came into general use. They
axe made of cast plates of brass, with the design worked
upon them with the chisel and graver. All those, how-
ever, to be seen in English churches are not of native
work — great quantities of them being Flemish imports (see
Cotman, Waller, and BouteU on Monumental Brasses).
In addition to its chief use as a roof covering, lead was
sometimes used in England for making fonts, generally
tub-shaped, with figures cast in relief. Many examples
'■xist : e.g., at Tidenham, Gloucestershire ; Warborough and
Dorchester, Oion ; Chirton, Wilts ; and other places.
Germany. — Unlike England, Germany in the 10th ana
11th centuries produced large and elaborate works in cast
bronze, especially doors for chuiches, much resembling
the contemporary doors made in, Italy under Byzantine
influence. Bernward, bishop of Hildesheim, 992-1022,
was especially skilled in this work, and was much influenced
in design by a visit to Rome in the suite of Otho III. The
bronze column \nX\i winding reliefs now at HUdesheim
was the result of his study of Trajan's column, and the
bronze door which he made for his own cathedi-al shows
classical influence, especially in the composition of the
drapery of the figures in the panels.
Fio. 7. — Part of one of the Hampton Court Gates.
The bronze doors of Augsburg (1047-72) are similar
in style. The bronze tomb of Rudolph of Swabia in
Mersburg cathedral (1080) is another fine work of the
same school. The production of works in gold and silver
was also carried on vigorously in Germany. The shrine of
the three kings at Cologne is the finest surviving example.
At a later time Augsburg and Nuremberg were the chief
centres for the production of artistic works in the various
metals. Herman Vischer, in the 15th century, and his son
and grandsons wereveryremarkable as bronze founders. The
font at Wittenberg, decorated with reliefs of the apostles,
was the work of the elder Vischer, while Peter and his son
produced, among other important works, the shrine of St
Sebald at Nuremberg, a work of great finish and of
astonishing richness of fancy in its design (see Doebner,
C/iristUches KunstUatt, 1866, Nos. 10-12). The tomb
of Maximilian I., and the statues round it, at Innsbruck,
begun in 1521, are perhaps the most meritoriotis German
work of this class in the 16th century, and show consider-
able Italian influence.
78
METAL-WORK
In wrought iron tho German smiths, especially during
the 15th century, greatly excelled. Almost peculiar to
Germany is the use of wrought iron for grave-crosses and
sepulchral monuments, of which the Nuremberg and other
cemeteries contain fine examples. Many elaborate well-
canopies were made in wrought iron, and gave full play to
ii»rt«c m\n
most are now destroyed, but a fine specimen still exists
at Westminster on tho tomb of William de Valence (1296).
In ornamental iron-work for doors the French smiths were
pre-eminent for the richness of design and skilful treatment
of their metal. No examples probably surpass those on
the west doors of Notre Darao in Paris^now unhappily
much falsified by restoration. The crockets and finiala
on the flfeches of Amiens and Eheims are beautiful speci-
mens of a highly ornamental treatment of cast lead, for
which France was especially celebrated. In most respects,
however, the development of the various kinds of metai-
j working went through much the same stages as in England.'
Persia and Damascus. — The metal-workers of the East?
e-speciaily in brass and steel, were renowned for their skill
-1 ilulU uij MI
the fancy and invention of tho smith. The celebrated
15th-century example over tho well at Antwerp, attributed
to Quintin Massys, is the finest of these.
France. — From the time of the Romans the city of
Limoges has been celebrated for all .sorts of metal-work,
and especially for brass enriched with enamel. In the
13th and 14th centuries many life-size sepulchral effigies
were made of beaten copper or bronze, and ornamented by
various-coloured "champlcv6" enamels. The beauty of
these effigies led to their being imported into England ;
Fig. 9. — Brass Vase, pierced and gUt ; 17th century Persian work.
even in the time of Theophilus, the monkish writer on the
subject in the 13th century. IBut it was during the reign
of Shah Abbas I. (d. 1628) that the greatest amount of
fikill both in design and execution was reached by the
Persian workmen. Delicate pierced vessels of gilt brass,
enriched by tooling and inlay of gold and silver, wer«
among the chief specialties of the Persians (see fig. 9).
A proce.ss called by Europeans "damascening" (from
Damascus, the chief sea' of tho export) was used to produce
very delicate and rich surface ornament. A pattern was
incised with a graver in iron or steel, and then gold wire
was beaten into the sunV lines, the whole surface being
then smoothed and polisbod. In tho time of Cellini this
process was copied in Itaiy, and largely used, especially
for tho decoration of weapons and armour. The repouss6
process both for brass and silver was much used by Oriental
workers, and even now fine works of this class are pro-
duced in the East, old designs still bein.j adhered to.
M E T — M E T
79
Seemi Metal- Worh — In modern Europe generally the
arts of metal-working both as regards design and tech-
nical bMI are not in a flourishing condition. The great
bronze lions of the Nelson monument in London are a sad
example of the present low state of the founder's art.
Coarse sand-casting in England now takes the place of the
delicate "cire perdue" process.
Some attempts have lately been made in (Jennany to
revive the art of good wrought-iron work. The Prussian
gates, bought at a high price for the South Kensington
Museum, a-e large and pretentious, but unfortunately are
only of value as P warning to show what wrought iron
ought not to be. Some ILngUsh recent specimens of ham-
mered work are more hopeful, and show that one or two
smiths are working in the right direction.
LiUraiure, — Pkehistoric : "Worsaae, Nordhke Oldsageri Kjoien-
havn, 1854 ; Perrin, itttde prehislorique—Age du brorne, 1870.
Classical : Layard, Nineveh and Babylon, 1853 ; Lane's aod
■Wilkinson's works on Ancient Egypt; Pliny, Natural History,
book x-xxiv. ; Brondsted, Den Fikoroniske Cisla, 1847 ; Daremberg,
Dictionnaire dea Anliquitis, "Coelatura," in course of publication ;
Gerhard, various monographs, 1843-67; Miiller, Etrusker, &c., and
other works; Ciampi, DelV Antica Tcreutica, 1815. Medieval:
Digby 'Wyatt, Metal- fVork of the Middle Ages, 1849 ; Shaw, Orna-
mental Metal- Work, 1836 ; Drury Fortnnm, S.K.M. Handbook of
Bronzes, 1877 ; King, Orfim-erie et ouvrages en metal du moyen
dge, 1852-4 ; Hefner-Alteneck, Serrurerie du moyen Age, 1869 ;
Viollet-le-duc, Diet, du -tnobilier, "Serrurerie" and " Oifevrerie,"
1858, &c. ; Lacroix, Tr6sor de S. Denis, and L'Art du moyen dge
(various dates) ; Karch, Die Ralhselbitder an der Brcmcethtlre zu
Augsburg, 1869 ; Krug, EntwUrfe fur Gold-, Silbcr-, und Bronze-
Arbeiter (no date) ; Linas, Orfimerie Merovingienne, 1864, and
Orfivrerie du XIII'^ SUcle, 1856; Bordeaux, Semirerie dti
moyen dge, 1858 ; Didron, Mamcel des osuvres de bronze el d'or-
fivrerie du moyen dge, 1859; Du Somraerard, Arts au 'tnoyen &ge,
1833-46, and Musie de Cluny, 1852 ; Durand, Tresor de Viglise de
Sainl Marc d Venise, 1862; Albert Way, Gold Rdahle of Basle,
1843; Rico y Sinobas, Trabajos de metales, 1871; Blanchard, Porto
du Baptisttre de Florence, 1868 ; Bock, Die Ooldschmiedekunst dcs
Mittelalters, 1855, and Kleinodien des Heil.-Riimischen JteicTtes ;
Jouy, Zes gemmes et les joyaux, 1865 ; Liibke, Works of Peter
Visscher, 1877 ; Adelung, Die ThUrcn zu S. Sophia in Novgorod,
1824 ; Wanderer, Adam Kraffl and his School, 1868 ; Nesbitt,
"Bronze door of Gnesen Cathedral," Arch. Jour., vol. ix.; Bossi,
Treporle di brmao di Pisa ; Digot, articles in Bulletin Uomtmental,
vols, xii -xvi. ; Catalogue of works of art in metal exhibited in
1861 at Ironmongers' Hal) ; Texier, Dictionnaire SOtfivrerie, 1867{
Virgil Solis, Designs for Gold- and Silver-Smiths, 1612 (facsimile
reproduction, 1862). PaAOTicAL Treatises: Tbeophilua, Diver-
sarum Artium Schedula; Cellini, Trattati delV Oreficeria e delta
Scultura; Vasari, Tre AHi del Disegjio, part ii, Milanesi's ed.,
1882; Gamier, Manuel du dseleur, 1869. (J. H. H.)
METAMOEPHOSIS. This term has been employed
in several distinct senses in biology. During the early
part of the century it was constantly used to include the
current morphological conceptions, as, for instance, of the
parts of a flower as modified or " metamorphosed " leaves,
or of the segments of a skull as mo<ified vertebrae.
It is still frequently employed to denote that progressive
change from the general to the special undergone by all
developing tissues and organs (see Biology, Embeyology),
but in this sense is conveniently superseded by the term
" difierentiation." In the process of animal development,
two types are broadly distinguishable, — a foetal type, in
which development takes place wholly or in greater part
either within the egg or within the body of the parent,
and a larval type, in which the young are born in a
condition more or less differing from that of the adult,
while the adult stage again is reached in one of two ways,
either by a process of gradual change, or by a succession
of more or less rapid and striking transformations, to
which the term metamorphosis is now usually restricted-
Metamorphosis is generally regarded as having been
brought about by the action of natural selection, partly in
curtailing and reducing the phases of development (ao
obvious advantage in economy of both structural and
functional change), and partly also in favouring the
acquirement of such secondary characters as are advan-
tageous in the struggle for existence. Freshwater and
terrestrial animals develop without metamorjfcosis much
more frequently than marine members of the same group,
a circumstance which has been variously explained. For
details of metamorphoses see the articles on the various
groups of animals; see also Balfour's Comparative Em-
bryology, 1880-81.
METAPHYSIC
THE term metaphysic, originally intended to mark the
place of a particular treatise in the collection of
Aristotle's works, has, mainly owing to a misunderstanding,
survived several other titles, — such as " First Philosophy,"
"Ontology," and "Theology," which Aristotle himself
used or suggested. Neo-Platonic mystics interpreted it
as signifying that whi^b is not mRrely "after" but
" beyond " physics, and found in it a flt designation
f<3r a aiience which, as they held, could not be attained
except by one who had turned his back upon the natural
world. And writers of a different tendency in a later
time gladly accepted it as a convenient nickname for
theories which they regarded as having no basis in
experience, in the same spirit in which the great German
minister Stein used the analogous title of " metapolitics "
for airy and unpractical schemes of social reform. A brief
indication of the contents of Aristotle's treatise may enable
ns to give a general definition of the science which was first
distinctly constituted by it, and to determine in what sense
the subjects which that science has to consider are beyond
"ature and experience.
For Aristotle, metaphysic is the science which has to do
with Being as such. Being in general, as distinguished from
the special sciences which deal with special forms of
Being. There are certain questions which, in Aristotle's
view, we have a right to ask in regard to everything that
presents itself as real. We may ask what is its ideal
nature or definition, and what are the conditions of its
realization ; we may ask by what or whom it was produced,
and for what end ; we may ask, in other words, for the
formal and the material, for the efficient and the final
causes of everything that is. These different questions
point to different elements in our notion of Being, elements
which may be considered in their general relations apart
from any particular case of their union. These, therefore,
the first philosophy must investigate. But, further, this
science of being cannot be entirely separated from the
science of knowing, but must determine at least its most
general principles. For the science that deals with what
b most universal in being is, for that very reason, dealing
with the objects which are most nearly akin to the
intelligence. These, indeed, are not the objects which are
first presented to our minds ; we begin with the particular,
not the universal, with a irpwrov rjfiiv which is not irpurrov
tj)v<Tci ; but science reaches its true form only when the
order of thought is made one with the order of nature, and
the particular is known through the universal. Yet this
conversion or revolution of the intellectual point of view
is not to be regarded as an absolute change from error to
truth ; for Aristotle holds that nikil est in iniellectv quod
turn priua in semu, in the meaning that in sense perception
there is already the working of that discriminative intelli-
80
M E T A P H Y S I C
gence' which, beginning in sense perception, with the dis-
tinction of particular from particular, can rest only when it
has apprehended things in their universal forms or defini-
tions. Looking at knowledge foiitiaUy, the highest law of
thought, the law of contradiction (or, as we might call it, to
indicate Aristotle's meaning more exactly, the law of de-
finition or distinction), is already implied in the first act of
perception by which one thing is distinguished from another.
Looking at it materiaUy, the reason of man is to be con-
ceived as potentially all that is knowable; i.e., objects are
so related to it that for it to know them in their essential
definitions is only to know itself. The aim of science, in
this view, is to break through the husk of matter, and to
apprehend things in their forms, in which they are one with
the mind that knows them. Hence also it follows that in
rising to the most universal science, the science of Being in
general, the mind is not leaving the region of immediate
experience, in which it is at home, for a far-off region of
abstractions. Rather it is returning to itself, apprehend-
ing that which is most closely related to itself, and which
therefore, though it is late in being made the direct object
of investigation, is yet presucposed in all that is. and is
known.2
Metaphysic, then, is the science which djeals with the
principles which are presupposed in all being and knowing,
though, they are brought to light only by philosophy.
Another trait completes the Aristotelian account of it.
It is theology, or the scienca of God. Now God is v6r]<Ti.<;
voijcrc<j5, pure self-consciousness, the absolute thought which
is one with its object, and Ho is therefore the first cause
of all existence. For, while the world of nature is a world
of motion and change, in which form is realized in matter,
this process of the finite can be explained only ty referring
it back to an unmoved mover, in whom there is no distinc-
tion of matter and form, and who is, therefore, in Aristotle's
view, to be conceived as pure form, the purely ideal or
theoretic activity of a consciousness whose object is itself.
Such a conception, however, while it secures the independ-
ence and absoluteness of the unmoved mover, by removing
him from all relation to what is other than himself, seems,
to make his connexion with the world inexplicable. We
can on this theory refer the world to God, but not God to
the world. Hence Aristotle seems sometimes to say that
God is the first mover oniy as He is the last end after which
all creation strives, and this leads him to attribufs to
nature a desire or mil «'hich is directed towards the good
as its object of end. '
Aristotle then brings together in his metaphysic three
elements which are often separated from each other, and
the connexion of which is far from being at once obvious.
It is to him the science of the first principles of being.
It is also the science of the first principles of knowing.
Lastly, it is the science of God, as the beginning and end
of all things, the absolute unity of being and thought, in
which all the differences of finite thought and existence
are either excluded or overcome.
To some this description of the conte'.\ts of Aristotle's
treatise, and especially the last part of it, may seem to be
a confirmation of all the worst charges brought against
metaphysic. For at both extremes this supposed science
seems to deal with that which is beyond experience, and
which therefore cannot be verified by it. It takes us
back to a beginning which is prior to the existence as well
as to the consciousness of finite objects in time and space,
and on to an end to which no scientific prophecy based
upon our consciousness of such objects can reach. In the
» Ai/)'a/iit KpiTtitl], Aval. Post., ii. 996.
^ AVhat is snid here as to the iutelligeoce is partly taken from the
De Animfu Tlie necessary qualifications of the above general state-
rM>i>» of Aristotle's views will le given subieqicntly.
former aspect of it, it has to do with notions so abstrtct
and general that it seems as if they could not be fixed or
tested by reference to any experience, but must necessarily
be the playthings of dialectical sophistry. In the iattc-
aspect of it, it entangles us in questions as fcs the final
cause and ultimate meaning of things, questions involving
so comprehensive a view of the infinite universe in which
we are insignificant parts that it seems as if any attempt
to answer them must be for us vain and presumptuous.'
On both sides, therefore, metaphysic appears to be an
attempt to occupy regions which are beyond the habitable
space of. the intelligible world — to deal with ideas which
are either so vague and abstract that they cannot be
fastened to any definite meaning, or so complex and far-
reaching that they can never by any possibility be verified.
For beings like men, fixed within these narrow limits of
space and time, the true course, it would seem, is Uy
"cultivate their gardens," asking neither whence they
come nor whither they go, or askir.g It only within the
possible limits of history and scientific prophecy. To go
back to the beginning or on to the end is beyond them,
even in a temporal, still more in a metaphysical, sense.
That which is npCnov <f>vcrei escapes us even more absolutely
than the prehistorical and pregeological records of man
and his world. That which is vmarov ijivau escapes us
even more absolutely than the far-off future type of
civilization, which social science vainly endeavours to
anticipate. Oiu- state is best pictured by that early
Anglican philosopher who compared it to a bird flying
through a lighted room "between the night and the
night." The true aim of philosophy is, therefore, it
would seem, to direct our thoughts to the careful exam-
ination and utilization of the narrow space allotted to us
by an inscrutable power, and with scientific self-restraint
to refrain from all speculation either on first or on final
causes.
The main questions as to the possibility and the nature of
metaphysic, according to Aristotle's conception of it, may
be summed up under two heads. We may ask whether
we can in any sense reach that which is beyond experience,
and, if so, whether this' " beyond " is a first or a last
principle, a pre-condition or a final cause of nature and
experience, or both. The former question branches out
into two, according as we look at metaphysic from the
objective or the subjective side, or, to express the matter
more accurately, according as we consider it in relation to
those natural objects which are mtrely objects of knovledgc,
or in relation to those spiritual objects which ire also
subjects of knowledge. We shall therefore consider meta-
physic, first, in relation to science in general, and, secondly,
in relation to the special science of psychology. The
latter question also has two aspects ; for, while the idea of
a first cause or principle points to the connexion between
metaphysic and logic, the idea of a last principle or final
cau[£ connects metaphysic with theolog)'. We shall there-
fore consider in the third place the relation of metaphysic
to logic, and in the fourth place its relation to religion and
the philosophy of religion. _
1. The Relation of Metaphysic to Science. — The beginnir/ga
of science and metaphysic are identical, though there is a
sense in which it may be admitted that the metaphysical
comes before the scientific or positive era. The first eflbrts
of philosophy grasp at once at the prize of absolute
knowledge. No sooner did the Greeks become dissatisfied
with the pictorial synthesis of mythology by which their
thoughts were first lifted above the confusion of particular
things, than they asked for one universal principle which
shoidd explain all things. The Ionic school sought to find
some one phenomenon of nature which might be used as
the key to all other phenomena. The Eleatics, seeing the
m. EiT A !> H Y !S I C"
81-
{utility of makinig oae finite thing the explanation oi au
other finite things, tried to find that explanation in the very
sotion of unity or being itself. We need not underestimate
the speculative value of such bold attempts to sum up all
the variety of the world in one idea, but it is obvious that
they rather give a nam4 to the problem than solve it, or
that they put the very consciousness of the problem in place
of the solution of it^ Science is possible only if we can
rise from thi3 particular to the universal, from a subjective
view of things as they immediately present themselves to
tis in perception to an objective determination of them
through laws and principles which have no special relation
to any particular set of events or to any one individual
subject. But this is only one aspect of the matter. To
advance from a conception of the world in ordine ad
■individuum to one in ordine ad universum, and so to
discount and eliminate what is merely subjective atid
accidental in our first consciousness of the world, is the
beginning of knowledge. But little is gained unless the
universal, which we reach through the negation of the
particulars, is more than their mere negation ; unless it
is a law or principle by means of which we can explain
the particulars. Now the defect of early philosophy
was that its universal was "the one beyond the many,"
not the "one in the many," — in other words, that it was
not a law or principle by which the particulars subsumed
under it could be explained, but simply the abstraction
of an element common to them. But the process of
knowledge is a process that involves both analysis and
synthesis, negation and reaffirmation of the particulars
with which we start. K we exaggerate the former aspect
of it, we enter upon the via negaliva of the mystics, the
way of pure abstraction and negation, which would open
the mind to the ideal reality of things simply by shutting
it to all the perceptions of sensible phenomena. And, if we
follow out this method to its legitimate result, we must
treat the highest abstraction, the aostraction of Being, as if
it were the sum of all reality, and the Neo-Platonic ecstasy
in which all distinction, even the distinction of subject and
object, is lost as the only attitude of mind in which truth
can be apprehended
In the philosophy of the Socratic school we find the first
attempt at a systematic as opposed to an abstract theory —
the first attempt to bring together the one and the many,
and so to determine the former that it should throw light
upon the latter. Yet even in Plato the tendency to oppose
the universal to the particular is stronger than the
tendency to relate them to each other, and in some of iiis
dialogues, as, e.g., in the Phsdo, we find a near approach
to that identification of the process of knowledge with
abstraction which is the characteristic of mysticism.
Aristotle, therefore, had some ground for taking the Platonic
principle that " the real' is the universal " in a sense which
excludes the reality of the individual. Yet, though he
detected Plato's error in opposing the universal to the
particular, and though, at the same time, he did not
entirely lose sight of the truth which Plato had exagger-
ated, that the particular is intelligible only through the
universal, Aristotle was not able to escape the influence
of that dualism which had marred the philosophy of his
predecessor. 'Hence the effect of his protest against a
philosophy of abstraction was partly neutralized by his
separation between the divine Being as pure form and
nature as the unity of form and matter, and again by his
separation of the pure reason which apprehends the
forms of things from the perceptions of sense which deal
with forms realized in matter. And after Aristotle's time
the tendency of philosophy was more and more to withdraw
from contact with experience. The Neo-Platonic philo-
fopl^, and the Christian theology which was so strongly
influenced by it, contained, indeed, an idea of the recon-
ciliation of God and nature, and hence of form and matter,
which -must ultimately be fatal to dualism, and therefore to
the method of mere abstraction. But the explicit meaning
of the philosophy of the Middle Ages was still dualistic,
and the mode in which the Aristotelian formuto were
wrought into the substance of Christian doctrine by the
scholastics tended more and more to conceal that idea of
the unity of opposites which was involved in Christianity.'
Hence medisevaJ realism presented, in its most one-sided,
form, the doctrine that " the real is the universal," meaning
by the universal nothing more than the abstract. And, as
a natural consequence, the modem insurrection of the
scientific spirit against scholasticism . took its start from
an equally bald and one-sided assertion of the opposite
principle, that " the real is the individual," meaning by
that the individual of immediate perception. If Platonism
had dwelt too exclusively on one aspect of the process of
knowledge, viz., that it seeks to rise above the particular, the
sensible, the subjective, to the universal, the intelligible, the
objectivie, as if in the latter alone were reality to be found,
modern men of science learnt from their fir.=it nominalistic
teachers to regard the universal as nothing more than an
abbreviated expression for the particulars, and science itself
as a mere generalization of the facts of sensible perception.
But. this view of scientific knowledge, as a mere reaffirma-
tion of what is immediately given in sense, is as imperfect
as the opposite theory, which reduces it to the mere
negation of what is so given. An ideal world utterly
and entirely divorced from the phenomenal, and an ideal
world which is simply a repetition of the phenomenal,
are equally meaningless. The processes of science have
both a negative and a positive side ; they involve a nega-
tion of the particular as it is immediately presented in
sense, but only with a view to its being reafiirmed with a
new determination through the universal. The fact as it
is first presented to us is not the fact as it is ; for, though
it is from the fact as given that we rise to the knowledge
of the law, it is the law that first enables lis to understand
what the fact really means. Our first consciousness of
things is thus, not an immovable foundation upon which
science may build, but rather a hjijothetical and self-con-
tradictory starting-point of investigation, which becomes
changed and transformed as we advance.
The nominalism of scientific men in modern times is due
to two special causes, one of which has already been
mentionei It is partly due to the traditions of a time
when medieval realism was the great enemy of science..
The Baconian protest against the " anticipation of nature ""
was a relative truth when it was urged against a class of
writers who supposed that true theories could be attained
without regard to facts ; the Baconian assertion of the
necessity of attending to axiomata media was the necessary
correction of the tendencies of mystics, who supposed that
philosophy could attain its end by grasping at once at
ab39lute unity, and contented themselves, therefore, with
a unity which did nothing to explain the differences.
But, when the former was turned into the dogmatic
assertion that the mind is, or ought to be, passive in the
process of knowledge, as having in itself no principle for the
explanation of things, and when the latter was turned intO'
the dogmatic assertion that science can only proceed from
part to part and never from the whole to the parts, these
relative truths became a source of error. And this error
was confirmed and increased by the mistaken views of those
who first tried to correct it. For these, admitting that
scientific truth is entirely derived from external experience,
only ventured to assert the existence of a priori knowledge
alongside of, and in addition to, that which is a posteriori.
In other words, they sought in inner exnerience a basis for
82;
MET A PHYSIC
those beliefs which outward c>q)er!sncij seemed uauble ; i
f^apport. But this basis was soon found to be troacLtrou3.
Introspection, observation of the inner life as opposed to
and distinguished from the outer life, could be only an
observation of the facts of the individual consciousness as
such; and to base religion and morality on such a founda-
tion was to treat God and right as subjective phenomena,
■which do not necessarily correspond to any objective
reality. Nor was this conclusion really evaded by the
assertion of the self-evidencing necessity of such ideas and
beliefs, or of the principles upon which they are founded.
For this necessity, as a subjective phenomenon, might be
accounted for otherwise than by the supposition of their
objective validity. Such scepticism, further, was favoured
by the progress of science, which, as it advanced from
I;hysic3 to biology and sociology, became more and more in-
consistent with the idea of an ■"•bsoluto breach between inner
and outer experience, and narrowed the sphere which had
iieen hitherto reserved for the former. Man, it '.vas urged, is
but a part in a greater whole, not exempted from the law
<_.f action and reaction which connects all parts of that
a-hole with each other. His individual life contains only
';, few links in a chain of causation that goes back to a
beginning and onward to an end of which he knows
nothing. And, as Spmoza says, vis qua unaquie'pie res in
existcndo perseverat a causis exicrnis injinite svperatt..
Hence to treat ideas which are only states of the individual
consciousness as the explanation of tJie world, instead cf
itreating them as phenomena to be explained by its relation
to that world, seemed to be an absurdity. The particular
beliefs and tendencies of the mind were to be regarded,
not as ultimate facts in reference to which everything
is to be interpreted, but rather as facts which are
themselves to be referred to more general causes and
laws. It thus appeared that the attempt to divide truth
into n.n a posteriori and an a priori part, the latter of
whio*) should find its evidence in an inner experience
as the former in an outer experience, is an illusive pro-
cess. If the a priori is reduced to the level of the a
posteriori, it becomes impossible to base on the a jmori
any beliefs that go beyond the range of subjective
experience. If the self and the not-self are taken simply
£3 different finite things, which we can observe in turn,
their relations must be brought vmder the general laws of
tha conne'rion of finite things with each other; and the
phenomena of miud must be treated, like the phenomena
of matter, as facts to be accounted for according to these
laws. I
But this of itself indicates a way of escape both from
the introspective theory and from the empiricism tb which
it is opposed. For it suggests the question — ^'\\Tiat is the
source of those very laws which guide the procedure of
gcienco in ;»':ounting for facts, psychological facts among
others? When a scieutiiSc psychologist of the modern
school attempts to show how by habituation of the
individual and the race the necessity of thought expressed
in the law of causation was produced i:i the minds of the
present generation of men, it is obvious that his whole
investigation and argument presuppose the law wboso
genesis he is accounting for. A glaring instance of such
circular reasoning is found in the writings of the most
prominent representative of the school in the present day.
Jlr Spencer begins by laying down as a first postulate of
science that necessity of thought must be taken as a
criterion of truth. It is by the continual aid of this
postulate that ho coiiolructs his system of nature, and
linally his psychological theory of the development of
consoiovsness in man. Yet the main object of this
psychological theory seems to be to account for the very
necessities with which the author starts. Obvioirsly such a
philosophy contains ekmc-ntj, of ivhich the author ia'
imperfectly conscious ; for it in^•olve3 that mind is not
only the last product but the first presupposition of
nature, or, in other words, that in mind nature retuma
upon its iii-st principle. But to admit this is at once to
lift the conscious being as such above the position which
ho would hold as merely a finite part of a finite world. It
is to assert that nature has an essential relation to a con-
sciousness which is developed in man, ajid that in tha
growth of this consciousness we have, not an evolution
which is the result of the action of nature as a system ot
external causes up/on him, but an evolution in which nature
is really " coming to itself," i.e., coming to self-conscious-
ness, in him.
Now it was Kant who first — though \n.\h. a certain
limitation of aim — brought this idea of the relativity
of thought and being to the consciousness of the modern
world. In the Critique of Pure JReason, thought, indeed,
is not set up as an absolute prim, in relation to which all
existence must be conceived, but it is set up as the pnus
of exiierience, and so of all existences which are objects of
our knowledge. Experience is for Kant essentially relativo
to the conscioiis self; it exists through the necessary
subsumption of the forms and matter of sense under the
categories, as, on the other hand, the consciousness of self
is recognized as essentially dependent on thjs process. On
this view, the a priori and a posteriori factors of experience
do not really exist apart as two separate portions of
knowledge. If they are severed, each loses all its mean-
ing. Perceptions in themselves are void ; categories in
themselves are empty. We do not look outwards for ona
kind of truth and inwards for another, cor do we even,
by an external process, bring facts given as contingent
under principles recognized as necessary ; but the a priori
is the condition under which alone the a posteriori exists
for us. Even if it is allowed that the facts of inner and
outer experience contain a cc<?ilingent element or matter,
given under the conditions of lime and space, yet neither
time nor space nor the facts of experience conditioned by
them exist for us except as elements of an experience
which is organized according to the categories.
This is the essejitip.l truth which Kant had to express.
It is marred in Lis statement of it by the persistent
influence of the abstract division between contingent
matter given from without and necessary principles
supplied from within, a division essentially inconsistent
with the attempt to show that the contingent matter ia
necessarily subsumed under these principles, and indeed
exists for us only as it is so subsumed. But Kant himself
puts into our hands the means of correcting his own
inadequacy, when he reduces the inaccessible thing in itself,
which he at first spsaks of as alTecting oui- sensibility and
so giving rise to the contingent matter of experience, to a
noumenon (movficvov) which is projected by reason itself.
The Dialectic exhibits the idea of thought as not only
constituting finite experience but also reaching beyond it,
though as yet only in a negative way. The mind is, on
this view, so far unlimited that it knows its own limits ; it
is conscious of the defects of its experience, of the con-
tingency of its sensible matter, and the emptiness and
Cniludo of its categories ; and by reason of this conscious-
ness it is always seeking in experience an ideal wbichit is
impossible to realize there. Thought measures experience
by its own nature, and finds it wanting. It demands
a kind of unity or identity in its objects which it is unable
to find in the actual objects of experience. It is this
demand of reason which lifts man above a mere animal
existence, and forces him by aid of the categories to
determine the matter of sense as a world of objects ; yet, aa
this finite world of experieuco can never satisfy the deouud
31 E T A P H Y S I C
83
of reason, thg consciousness of it is immediately com-
bined with the consciousness of its limited and phenomenal
character. The student of the Critique of Pure Reason
cannot but recognize the strange balance between the real
and the phenomenal in which it ends, allowing to man the
consciousness of each so far as to enable him to see the
defects of the othfer, — so that by aid of the pure identity of
reason ho can criticize and condemn the " blindness " or
unresolved difference of experience, and by means of the
concreteness and complexity of experience he can condemn
ithe " empty " identity of reason.
In order, however, to understand the full bearing of
Kant's criticism of knowledge, and at the same time to find
■the meeting-point of the opposite currents of thought which
alternately prevail in it, it will be necessary to consider
the subject a little more closely. The lesson of the Critique
may be gathered up into two points. In the first place,
it is a refutation of the ordinary view of experience as
Bomething immediately given for thought and not con-
stituted by it. In the second place, it is a demonstration
of the merely phenomenal character of the objects of
experience, i.e., the demonstration that the objects of
experience, even as determined by science, are not things
in themselves. Both these results require to be kept
clearly in view if we would understand the movement of
thought excited by Kant. On the one hand Kant had to
teach that what is ordinarily regarded as real, the world
of experience, is transcendently ideal, i.e., is determined as
real by a priori forma of thought. On the other hand he
had to teach that the world so determined is empirically
and not transcendentaUy real, i.e., its reality is merely
phenomenal. With the former lesson he met the man of
science, and compelled him to renounce his materialistic
explanation of the world as a thing which exists in
independence of the mind that knows it. The world we
know is a world which exists only as it exists /or us, for
the thinking subject; hence the thinking subject, the ego,
cannot be taken as an object like other objects, an object
the phenomena of which are to be explained like other
phenomena by their place in the connexion of experience.
Having, however, thus repelled scientific materialism by
the proof that the reality of experience is ideal, Kant
refuses to proceed to the complete identification of reality
with ideality, and meets the claims of the metaphysician
with the assertion that the reality of e.xperience is merely
phenomenal. Hence he rejects any idealism that would
involve the negation of things in themselves beyond
phenomena, or the identification of the objects of experience
with these things. The reality we kno-v is a reali^ which
exists only for us as conscious subjects, but this, though
it is the only reality we can know, is not the absolute
reality.
It is, however, to be observed that the nature of this
opposition between phenomena and things in themselves
seems to change as we advance from the Analytic, where
the existence of such things is presupposed, to the Dialectic,
where the grounds of that presupposition are examined.
At first the opposition seems to be between what is present
in consciousness and what is absolutely beyond conscious-
ness. The matter of experience is regarded as given exter-
nally in the affections of the sensibla subject, — affections
caused by an unknown thing in itself, of which, however,
they can tell us nothing. On the other hand the form of
experience; the categories and principles of judgment which
turn these affections into objects of koowlidge. are not pure
expressions of the real natiire, the pure identity, of the
subject in itself, but only product? of the identity of the
.self in relation to the sensibility and its forms of time
and space. Hence, on both sides we must regard expe-
jieoca as merely phenomenal, alike in relation to the
noumenal object and in relation to the noumenal subject,
which lurk behind the veil and send forth into expe-
rience on the one side affections which become objects
through their determination by the unity of thought, and
on the other side an identity of thought which becomes
self-conscious in relation to the objects so determined by
itself.
Kant, however, having thus answered the question of
the possibility of exiierience by reference to two things in
themselves which are out of experience, is obliged to ask
himself how the ronscicvsness of these two things in
themselves, and the criticism of experience in relation to
them, is possible. And here, obviously, the opposition
can no longer be conceived as an opposition between that
which is and that which is not in consciousness. For the
things in themselves must be present to consciousness in
some fashion in order that they may be contrasted ^-ith the
phenomena. If, therefore, phenomena are now regarded
as unreal, it m\ist be because we have an idea of reality to
which the reality of experience dos3 not fully correspond.
In the Analytic Kant had beenispeaking as if the real con-
sisted in something which is not present to the conscious
subject at all, though we, by analysis of his experience,
can refer to it as the cause of that which is so present.
Now in the Dialectic he has to account for the fact that
the conscious subject himself is able to transcend his
experience, and to contrast the objects of it as phenomenal
with things in themselves.
Now it is obvious that such an opposition is possible only
so far as the thought, which constitutes experience, is- at
the same time conscious of itself in opposition to the
experience it constitutes. The reason why experience is
condemned as phenomenal is, therefore, not because it is
that which exists for thought as opposed to that which
does not exist for thought, but because it imperfectly
corresponds to the determination of thought in itself. In
other words, it is condemned as unreal, not because it is
ideal, but because it is imperfedly ideal And the absolute
reality is represented, not as that which exists without
relation to thought, but as that which is identical with the
thought for which it is. In the Dialectic, therefore,
the noumenon is substituted for the thing in itself, and
the noumenon is, as Kant tells us, the object as it exists
for an intuitive or perceptive understanding, i.e., an under-
standing which does not synthetically combine the given
matter of sense into objects by means of categories, but
whose thought is one with the existence of the objects it
knows. It is the idea- of such a pure identity of knowing
and being, as suggested by thought itself, which leads us
to regard our actual empirical knowledge as iinperfect, and
its objects as not, in an absolute sense, real objects. The
noumena are not, therefore, the unknown causes by whose
action and reaction conscious experience is produced ; they
represent a unity of thought with itself to wliich it finds
experience inadequate. This higher unity of thought with
itself is what Kant calls reason, and he identifies it with
the faculty of syllogizing. Further, he finds in the three
forms of syllogism a guiding thread which brings him to
the recognition of three forms in which the pure unity of
reason presents itself to us in opposition to the merely
synthetic unity of experience, a psychological, a cosmo-
logical, and a theological form. In each of these cases
the empirical process of knowledge is accompanied, guided,
and stimulated by an idea which nevertheless it is imable
to realize or verify. In psychology we have ever present
to us an idea of the identity of the self, which is never
realized in our actual self -consciousness, • because the self
of which we are conscious is manifold in its states and
because it stands in relation to an external world. The
idea of simple identity ic, therefore, something we may set
34
METAPHYSIC
before us aa tho goal r4 an ideal psychology, to which we
may approximate in bo far as we can trace unity of faculty
tbroufjh all the diiTorences of mental phenomena, but tr
which we can never attain owing to the nature of the matter
witi which we deal. Again, in our scientific attempts to
explain our external experience, the unity of reason takes
the form of aa idea of the world as a completed infinite
whole, which contains all the objects known to us and all
other possible objects ; but this cannot be realized in
an experience which is conditioned by space and time,
and is, therefore, ever incomplete. The idea of totality
)s, therefore, an ideal, which guides and stimulates our
scientific progress, without which such a thing as science
could not exist, but which at the same time can never be
realized by science. Lastly, the unity of reason takes a
third form in which identity and totality are combined, —
as the idea of a unity in which all differences, even the
difference of subject and object, are transcended, — the idea
of a unity of all things with each other and with the mind
that knows them. This idea also is one which science can
neither surrender nor realize. It cannot surrender it
without giving up that striving after unity without which
science would not exist ; and it cannot realize it, for tne
difference between the world, as it is presented to us in
actual experience, and the subjective determination of
our thinking consciousness cannot be overcome. We can,
indeed, use the idea that the world is an organic whole,
determined in relation to an end which consciousness sets
for itself, as an heuriMic principle to guide us in following
the connexion of things with each other ; but, as we cannot
by means of any such idea anticipate what the facts of
external experience will be, so we cannot prove that for a
mind other than ours the unity of things which we repre-
sent in this way might not take a quite different aspect.
Indeed we have reason to think it would ; for, while we
always think of a designing mind as using materials which
have an existence and nature independent of the purposes
to which they are put, the absolute mind must be conceived
as creating the materials themselves by the same act
whereby they are determined to an . end. We must con-
ceive it, in short, as an intuitive understandimi for which
end and means, objective and subjective, aiv one, or, in
other words, as an intelligence whose consciousness of
itself is or contains the existence of all that is object
for it.
This new view of the things in themselves as noumena
or ideals of reason involves a new atfitude of thought
towards them different from that dogmatic attitude which
is provisionally adopted in the Analytic. Accordingly, wo
now find Kant speaking of them, not as things which exist
independently of their being conceived, but as " prob-
lematical conceptions " of which we cannot even determine
whether they correspond to any objects at all. They are
"limitative " notions which have a negative value, in so far
as they keep open a vacant space beyond experience, but
do not enable us to fill that space with any positive realities.
They are like dark lanterns which cast light upon the
empirical world, and show what are its boundaries, but
leave their own nature in obscurity. All that we can say
of the noumenal self or subject is that it corresponds to the
unity implied in all knowledge, but whether there is such
a self, independent of the process of empirical synthesis
and the self-consciousness which accompanies that process,
we cannot tell. All tliat we can say of the noumenal reality
of tho objective world is that it corresponds to the idea
of the objects of experience as a completed whole in them-
selves apart from the process whereby we know them, but
whether there is any such real world independent of tho
process of experience it is impossible to say. Lastly, all
that we can say of God is that He corresponds to the idea
of the unity of all things with the mind that Knows them, —
an ideal which is involved in all knowledge, — but whether
the realization of this idea in an intuitive understanding
is even possible we have no means of determining, how-
ever Wi, msv suspect that understanding and sensibility are
" branches springing from the same unknown root." The
Criticism of Purt, Reason ends, therefore, in a kind of
seesaw between two for.-ns of consciousness — a thinking
consciousness, which trauEcenls experience and sets before
us an idea of absolute reality, but which cannot attain
to any knowledge or even certitude of any object
corresponding to this idea, and an empi-'cal conscious-
ness, which gives us true knowledge of its objects, but
whose objects are determined as merely phenomenal and
not absolutely real.
The equipoise thus maintained between tho empirical
and the intelligible world is, however, in the Critique of
Practical Reason, overbalanced in favour of the latter.
What tho theoretical reason could not do " in that it was
weak through the flesh," through its dependence on the
very empirical consciousness which it sought to transcend,
is possible to the practical reason, because it is primarily
determined by itself. In our moral consciousness we find
ourselves under a law which calls upon us to act as beings
■who are absolutely self-determined or free, and which,
therefore, assiu-es us that our intelligible self is our real self,
and conclusively determines our empirical self in contrast
with )'i, as phenomenal. Thus the moral law gives reality
to the intelligible world ; or, as Kant expresses it, " the
idea of rn intelligible world is a point of view beyond the
phenomepal which the reason sees itself compelled to take
up, in order to think of itself as practical." In other
words, the moral law presupposes freedom or determination
in the rational being as such, and makes him regard him-
self, not me ply as a link in the chain of conditioned
existences in •ime and space, but as the original source
of his own life. The blank space beyond the phenomenal
thus begins to b? filled up by the idea of a free causality
which again po tulates a world adequate and conform-
able to itself. And the man who, as an empiric individu-
ality, is obliged to regard himself merely as an individual
being determined by other individual beings and things
is authorized as a noral being to treat this apparent
necessity as having its reality in freedom, and to look upon
himself as the denizen of a spiritual world where nothing
is determined for him from without which is not simply
the expression of his o "n self-determination from within.
" Thus we have found, what Aiistotle could not fiod, a
fixed point on which reason can set' its lever, not in any
present or future world, but in its own inner idea of
freedom, — a point fixed f r it by the immovable moral
law, as a secure basis from which it can move tho human
will, even against the opposition of all the powers of
nature." * Starting from this idea of freedom, therefore,
Kant proceeds to reconsti'uct 'or faith the unseen world,
which in tho Critique of Pure Reason he had denied as an
object of kncfivledge. Nor is he content to leave the
two worlds in sharp antithesis t? each other, but even in
tho Critique of Practical Reason, and still more in the
Critique of Judgment, he brings them into relation to each
other, and so gives to theoretical reason a kind of
authority to use for the explanation of the phenomenal
world those ideas which of itself it might be inclined to
regard as illusive.
In all this, however, it is difficuK to avoid seeing a
partial retractation of Kant's first view as to the irreconcilable
opposition of the phenomenal and tho noumenal. For, in,
the first place, the moral imperative is a-" dressed to a self'
' KAiit, i. G33 (Roscnkraiu'e e\Ution .
METAPHYSIC
85
itrUch is at one and the same time regarded in both
jbharacters, and which is called upon to subsume under the
(moral law acts which otherwise derive their character and
Imeaning from the relations of the phenomenal world. That
ithe particular nature of men as phenomenal individuals
jean be the means of realizing the universal law of reason is
implied in all Kant's statements of the latter, and particu-
larly in his conception of men as constituting together a
"kingdom of ends"; for it is difficult to conceive this
kingdom otherwise than as an organic unity of society, in
■which each individual, by reason of his special tendencies
and capacities, has a definite office to fulfil in realizing
the universal principle that binds all the members of the
tin^dom to each other. The summum bormm, again, is
said to consist in the union of happiness with goodness,
i.e., of the empirical conditions of man's individual life as
a sensible subject with the pure self-determination of the
intelligible self j and God is postulated as a Deus ex
macJiina to bind together these two unrelated elements, —
a conception which shows the difficulty into which Kant
has brought himself by defining them as unrelated. Still
more obvioiis is the effort of Kant to get beyond the
dualism of his first view of things in the Critique of
Judyment. For in that work he maintains that the con-
sciousness of the beautiful and the sublime is or involves
a harmony of the understanding or the reason with sense ;
and, what is still more important, he points out that the
idea of organic unity, without which we cannot explain the
phenomena of life, contains in it a possibility of the recon-
ciliation of freedom and necessity, of the intelligible and the
phenomenal. This idea, he argues, we are authorized by
our moral consciousness to apply to the whole course of the
things in the phenomenal world, and so to regard it as a
process to realize the moral ideal. No doubt he again
partially retracts this view when he declares that we must
treat the idea of final causality as merely a subjective
principle of judgment, which, even in the case of living
beings, is to be regarded only as necessary for us as finite
intelligences. But such saving clauses, in which Kant
recurs to the dualism with which he started, cannot hide
from us how near he has come to the. renunciation of it.
When we regard Kant in this way as asserting from one
point of view an absolute limit which from another point
of view he permits us to transcend, it becomes obvious
that his philosophy is in an unstable equilibrium, which
cannot but be disturbed by any one who attempts to
develop or even to restate his ideas. Hence we need not
wonder that those who take in earnest his denunciations
of any attempt to transcend experience generally, — like
Professor Hukley, — reject as worthless all Kant's later work ;
and that, on the other side, those who take in earnest his
ideas of freedom, of organic unity, of an intuitive under-
standing, and of a summum bonnm in which freedom and
necessity meet together, are compelled to break through
the arbitrarj' line which he drew between knowledge
and belief. In favour of the former course it is easy in
many places to appeal to the letter of Kant. In favour of
the latter it need orJy be pointed out that, in Kant's view,
all experience rests upon, or is in its development guided
by, those ideas which yet he wiU not permit us to treat as
sources of knowledge. Hence the principles of the Critique
cannot legitimately be used against metaphysic, except
by those who are prepared to admit the ideas of reason, up
to the point to which he admits them, as ideas that limit
and direct our experience, — while rejecting all use of them
to cast light upon that which is beyond experience. In
other words, they must maintain the possibility of a purely
negative knowledge, of the knowledge of a limit by one
,who yet cannot go beyond it. They must show how we
.can have an ideal of knowledge which enables us to criticize
experience without enabling us to transform it ; they mn.^t
show how ideas of the supersensible can so far he present
to our thought as to make visible the boundaries of the
prison of sense in which we are confined, without in any
way enabling us to escape from it.
Is this possible? We may gather up the Kantian
antithesis in the assertion that experience is the imperfect
realization of aa ideal of knowledge, derived from reason,
with materials, derived from sense and understanding, the
nature of which is such that they can never be brought
into correspondence with the ideal. But this ideal, in all its
throe forms, as we have seen, is simply the idea of a pure
unity or identity in which all differences are lost or
dissolved — whether they be the differences of the inner or
of the outer life, or finally the difference of inner and
outer, subjective and objective, from each other. Kant's
view therefore is, in effect, this, that thought carries
with it the consciousness of an identity or umty, to whic'a
our actual experience in none of its forms fully coiTesponds.
On the other hand, Kant does not hesitate equally to con-
demn the identity of thought as " empty ' and subjective,
because it does not contain in itself nor can evolve from
itself the- complex matter of experience. But this
alternate condemnation of experience as unreal from the
point of view of the ideas, and of the ideas as umeal from
the point of view of experience, seems to show that hoOt are
unreal, as being abstract elements, which have no value save
in their relation to each other, and which lose all their mean-
ing when separated from the unity to which they belong
According to tliis view, ideas and experience, noumena
and phenomena, if they are opposed, are also 'necessarily
related to each other. If our empirical consciousness of
the world of objects in space and time, as determined by
the categories, does not correspond to the unity or identity
of thought which is our ideal of knowledge, yet that idea
of unity or identity is set up by thought in relation to
experience, and cannot, therefore, be essentially irrecon-
cilable with it. The two terms may be opposed, but their
opposition cannot be absolute, seeing that they are in
essential relation to each other. It is a great logical error
not to discern that a negative relation is still a relation,
i.e., that it has a positive unity beyond it. This positive
unity may not, indeed, be consciously present to us in
our immediate apprehension of the relation in question,
but it is necessanly implied in it. Now it is just because,
in his separation of noumena and phenomena, Kant omits
to note their essential relativity that he is forced to regard
the former as a set of abstract identities of which nothing
can be known, and the latter as the imperfect products of
a synthesis which can never be completed or brought to a
true unity. Yet the value of his whole treatment of the
ideas of reason in relation to our intellectual and moral
experience arises from the fact that in practice he does
not hold to this abstract separation of the two elementa
Ideas absolutely incommensurable with experience could
neither stimulate nor guide our empirical synthesis ; they
could not even be brought into any connexion with it.
When, therefore, Kant brings them into this connexion, he
necessarily alters their meaning. Hence the pure abstract
identity which excludes all difference is changed, in its
application, into the idea of an organic unity, of which the
highest type is found in self-consciousness, with its trans-
parent difference of the subjective and objective self. It
would be absurd and meaningless to say that science seeks to
reduce experience to an abstract identity, in which there is
no difference, unless for this were tacitly substituted what
is really an entirely different proposition, that science seeks
to find in the infinitely diversified world of space and time
that unity in difference of which self<onBciousness has in
itself the pattern. It is in reference to the former land
(86
METAPHYSIC
of identity — the abstract oneness of formal logic — tbat '
Kant proves that it is impossible for experience to be .
made adequate to ideas. But it is only of the latter kind
of identity — the oneness of seLf-consciousness — that it can
be said that it furnishes a guiding principle to scientific
investigation or an ideal of knowledge. The same con-
fusion is still more evident in Kant's account of our moral
experience, in dealing with ivhich he directly attemjits to
get sjnithetic propositions out of the pure identity of
reason, in tjther words, to draw, definite moral laws out
of the logical principle of non-contradiction. Whatever
success he attains is gained by substituting for the formal
principle of self-consistenct/ the positive idea of conaistcncy
with the self, and again by conceiving this self as a concrete
individual, the member of a society, and so standing in
essential relation to other selves. The pure abstraction
from all the external results of action and from all motives
of desire, which at the beginning of the Metaphi/sic of
Ethics Kant declares to be essential to moralitj', is modified
and indeed transformed, as we go on, by the admusious
that other rational beings are not external to us in any
sense that excludes their good from being an end of our
endeavour, and that the desires are not irrational and
immoral except in so far as they are directed to the
pleasures of the sensuous individual (which in a conscious
being they never entirely are). Both in the speculative
and in the practical sphere, therefore, the absolute opposi-
tion of the ideal or noumenal to the empirical disappears,
as soon as Kant attempts to apply it. For in both the
abstract identity of formal logic, which is really the
meaning oi the noumenon as absolutely opposed to and
incommensurable with experience, gives way to the unity
of self -consciousness, — a unity which is so far from being
absolutely opposed to the" difference of the empirical
consciousness that it necessarily implies it. For self-
consciousness presupposes the consciousness of objects ;
though it is opposed to that consciousness, it is essentially
correlated with it, and therefore its oppo:;ition cannot be
regarded as absolute, or incapable of b^ing transcended.
These considerations may throw some light on the
relation of the Analytic and Dialectic of Kant, and on the
nature of the opposition of noumenon and phenomenon
as it is presented in the latter. In the deduction of the
categories, Kant pointed out the ci.sential relation of the
objective world of experience to what he called the
"transcendental unity of apperception"; i.e., he pointed
out that the unity of coasciou'.ness is implied in all its
objects. This unity, he further showed, must be conceived
as "capable of self-consciousness"; but it actually becomes
conscious of self only in relation, though also in oppcei-
tion, to the other objects determined by it. Now it is this
consciousness of itself in opposition to other objects which
is the source of Kant's " ideas of reason," of the dissatisfac-
tion of the mind with its empirical knowledge, even in its
EcientiQo form, and of the demand for a higher kind of know-
ledge to which experience is not adequate. That a standard
is set up for c;qierience by which it is condemned is simply
a result of the further development of that unity which is
implied in experience — a result of the progress of thought
from consciousness to self-consciousness, and of the contrast
between the former and the latter. The problem with
which Kant's Dialectic attempts to deal, and which it treats
as insoluble, is, therefore, simply the problem of raising con-
sciousness to the form of sclf-consciotisness ; in other words, of
attaining to a knowledge of the world of experience as not
merely a " synthetic,"and therefore imperfect, unity of things
external to each other, but as an organic unity of transparent
differences, a self-difTercntiatinjr,, Erlf-inlcgrating unity, such
as seems to be presented to us in pure self-consciousness.
Nor can this problem bo regarded as insoluble; for the
unity of self-consciousness is identical with the unity of
consciousness ; it is only that unity become self-conscious.
Hence the point of view at which consciousness and self-
consciousneis .ceem to be absolutely opposed to each other, —
the highest point of view which Kant distinctly reaches, —
can be regarded only as a stage of transition from the point
at which their relative difference and opposition is not v>-t
developed to the point at which they are seen to be I'je
factors or elements of a still higher unity.
The later philosophy of Germany, from Kant to Heg.;L
is little more than the development of the idea just stated
in its twofold aspect. In the first place, it is an attempt
to show what is involved in the idea of thought or self-
conscioumess as in itself an organic whole, a manj'-in-one,
a unity which expresses itself in difference, yet so that the
difference remains transparent, and therefore is immediately
recognized as expression ot the unity. In the seconHf,
place, it is an attempt to bridge over the difference between
thought or self-consciousness and the external world of
experience, and to show that this opjiosition also is
subordinated to a higher unity. Or, to put it more directlj",
the idealistic philosophy of Germany seeks, on the one
hand, to develop a logic or metaphysic which bases itself,
not, like formal logic, on the idea of bare identity, but on
the idea of self-consciousness; and, on the other hand, to
show, in a philosophy of nature and spirit, how, by mean.?
of this logic, the opposition of thought to its object, ot
of the a priori to the a jjostcriori in knowledge, may ba
transcended. In the third and fourth sections of this
article Eomet'uing more will be said of the manner in
which this task was fulfilled. Here only a few words are
necessary to sum up the results reached, and to give more
distinctness to the new ideal of knowledge which th-s9
results suggest. We have seen that Kant's critical attitude
involved two things,— on the one hand, the assertion that
the existence we know is necessarily existence for thought,
and, on the other hand, the denial that that which exi.aj
for our thought is ab.solute reality, a denial which again
involves the presence to our thcfUght of an ideal of know-
ledge, by which our actual knowledge is condemned.
This ideal, however, was falsely conceived by Kant as an
identity without any difference, and, in this sense, he does
not hesitate to apply it even to self-consciousness itself.
For, in a remarkable passage,' be attempts to prove that
the consciousness of self is not a knowledge of the self, by
a simple reference to the duality of the self knowing and
the self known, arguing that the ego " stands in its o-ivn
way," just because it exists only /or itself, i.e., because in
knowing itself it presupposes itself. Kant evidently thinks
that to know the real self it would be necessary to apprehend
it in simple identity as purely an object without reference
to a subject, or purely a subject without reference to an
object. Yet to this it seems sufficient to answer that ."ich
an object or subject would lose its character as object cr
subject and become equivalent to mere being in general,
and that, as such being is a mere abstraction, to know it
cannot be the ideal of knowledge. If therefore there be a
unity or identity of thought which is not realized in ex-'
perience, and in reference to which wc can regard experience
as an imperfect form of know ledge, it cannot be found in
this abstract identity of being. In truth, as we have seen, it
is found in that very idea of self-consciousness which Kant
is criticizing. Just because we are self-conscious, and thtre-^
fore oppose the unity of' the conscious self to the nianifold-
ness of the world in space and time, do we seek in the'
world of space and time for a transparent unity which w^
cannot at first find there. But, when this is seen, we find
in Kant himself the partial solution of the diflSculty.
' Erica-, p. 279 (Eosenkrmz's edition), <^. Hegel, v. p. 258.
METAPHYSIC
m
BslZ-fOiisciousnesa presupposes consciousness ; for, while the
•pu^ebensioQ of objects in consciousness is possible only
in relatioa to the unity of the self, yet it is only in
lelatioa to and distinction from these objects that we are
conscious of that unity. Hence the two opposites, self
and not-self, arc bound together, and presuppose a unity
»b:ch rcv^aU itseli in luen opposition, aud which, wUen
made explicit, must reconcile them. If, therefore, self-
fonscioussess, in its first opposition to consciousness, gives
rise to an ideal of knowledge to which our empirical
knowledge of objects is inadequate, this arises from the
(act that not only empirical knowledge but also the ideal
to which it is opposed is imperfect, or that they both
point to a unity which is manifested in their difference,
and which is capable of containing and resolving it. In
other words, the opposition of science to its ideal, which
Kant has stated in his Antinomies, is not an absolute
opposition, but one the origin and end of which can be
aeen.
This opposition reaches its highest point in the con-
trast between the transparent unity of self<onsciousnos3,
in which the difference of knower and known is evanescent,
and the essential manifoldness and self ■e.xternality of the
vorld in space, iik which the differences seem to be insoluble.
We must, indeed, think of self-consciousness as having life
in itself and therefore as differentiating itself from itself ;
but this differentiation is held within the limit of its unity,
it is a separation of movements which are separated only as
they are united. On the other hand, the world in space
presents itself as the sphere of external determination, in
which things are primarily disunited and act only as they
are acted on from without, and in which this external
influence never goes so far as to destroy their reciprocal
externality. In this sense it is that the opposition of mind
and matter was taken by Descartes, and it is a survival of
the same mode of thought that leads many even now to
draw absolute lines of division between a priori and a
posteriori, between ideas and facts, between spiritual and
natural. Kant and Fichte give a new aspect to the
difficulty by showing that the difficulty is one of recon-
ciling consciousness and self-consciousness, and that in
tonsciousness there is already present the unity which is
manifested in self-consciousness, as, on the other hand, it
is only through consciousness and in opposition to it that
«elf-consciousnes3 is possible. And Fichte made a further
■tep when he attempted to show that the categories and the
forms of perception, 'time and space, which Kant had taken
as inexplicable facts, are implied in this contrast of con-
iciousness and self-consciousness. The error that clings to
Fichte's spoculatidns is, however, that he treats conscious-
ness merely as a necessary illusion which exists simply
with a view to self-consciousness, and hence is led to regard
eelf-consciousness itself — because it is essentially related
to this necessary illusion — as a schema or image of an
■nknowable absolute. In fact, in the end Fichte falls
back upon the abstract identity in which Kant had found
his noumenon, and so ends his philosophy with mysticism.
Even Schelling, though he saw that the absolute unity
must be one that transcends the difference of self and not-
»elf, did not finally escape the tendency to merge all
iifference in absolute oneness. On the other hand, it was
file endeavour of Hegel to proceed in the opposite way, —
Bot to lose self -consciousness or subjectivity in a mere
■nity of substance, but rather to show that the absolute
•ubstance can be truly defined only as a self-conscious
■nbject. And just because he did this he was prepared
to take a further step, and to regard the external world,
■ot as Fichte regarded it, as merely the opposite of spirit,
*D«' as Schelling regarded it, as merely the repetition and
«>-eqtjal of sgirit, but rather as its necessary manifestation
or as tnat in and througn which alone it can realize itself.
His doctrine therefore might be summed up in two proposi-
tions,— first, that the absolute substance is spiritual or self-
conscious, and, secondly, that the absolute subject or spirit
can be conceived as realizing itself only through that very
world of externality which at first appears as its opposite,
in both respects Hegel's philosophy reverses the via nrga-
iiva of mysticism, and teaches that it is only through the
exhaustion of difference that the unity of science, of which
the mind contains in itself the certitude, is to be realized.
For mind or spirit, viewed in itself, is conceived as a self-
differentiating unity, a unity which exists only through
opposition of itself to itself. And it is but a necessary
result of such a conception that spirit can fully realize its
unity only through a world which in the first instance
must present itself as the extreme opposite of spirit.
Hence the process of thought in itself, which is exhibited
in the logic, ends in the opposition to thought of a world
which is its negative counterpart. And the "absolute
spirit " of Hegel is thus, not pNire self-consciousness, but
that more concrete unity of self-consciousness with itself
which it attains through and by means of this world.
The effect of this view upon the relation of metaphysic to
science, which we are at present considering, is noticeable.
It does not, as is often supposed, supersede science by an
a priori construction of the universe, nor does it leave the
results of science unchanged and simply provide for it a
deeper, foundation. The latter was the point at which
Kant md Fichte stopped ; for, while they showed the
■ relativity of experience to the principle of self-consciousness,
they conceived that the function of metaphysic is completed
in showing the phenomenal character of the objects of
science, and in reserving a free spare beyond the phe-
nomenal world for " God, freedom, and immortality."
Schelling, on the other hand, a.i he did not adopt this
merely negative view of the relation of .ipirit to nature or
of a priori to empirical truth, was obliged to reinterpret
the latter by the former. As, however, ho did not recog-
nize any distinctions which were not merely quantitative,
he was led to apply the same easy key to every lock, and
to think that ho had explained all the different forms of
existence, organic and inorganic, when he had merely
pointed out a certain analogy between them. The meta-
physic of Hegel, whatever may be said of the actual
philosophy of nature produced by its author, contains no
necessity for any such arbitrary procedure. In his Logic,
indeed, he attempts to give us in ahstracto the movement
of thought in itself, from its simplest determination of
being as qualitative or quantitative, through the reflective
categories of substance and cause, up to its full conscious-
ness of itself in its organic unity.' And in so doing he of
course gives us an account of the various categories which
science uses in the interpretation of nature. He further
attempts to show that the highest categories of science are
in themselves imperfect and self-contradictory, — in other
words, that they mark a stage of thought which falls
short of that unity of being and knowing after which
science is striving, and which is the presupposition as
well as the goal of all intelligence. But, while he does
this, he clearly acknowledges two things, — on the one
hand that nature is essentially different from pure self-
consciousness, and that therefore logic can never by
direct evolution of its categories anticipate the investiga-
tions of science, and, in the second place, that the final
interpretation of nature through the highest categories
presupposes its interpretation by the lower categories, and
cannot be directly achieved without it. In other words,
' This nabjuct— the prsgreaa of .tl.oaght from lower to higher cato-
gorios sad mothods — wiU be more iully discussed in the third section.
88
METAPHYSIC
science must first dcturmine the laws of nature according
to the principles of causality and reciprocity, ere philosophy
can be in a position to discover the ultimate meaning of
nature by the aid of higher principles. " The philosopliy
of nature," says Ilegel, "takes up the material which
physical science by direct dealing with experience has
jjrepared for it at the point to which science has brought
it, and again transforms this formed material without
going back to exi^erience to verify it. Science must,
therefoie, work into the hands of philosophj^ in order that
philosophy in its turn may translate the lower universality
of the understanding realized by science into the higher
universality of reason, and may show how in the light of
this higher universality the intelligible world takes the
aspect of a whole which has its necessity in itself. The
philosophic way of looking at things is not a capricious
attempt, once in a way for a change, to walk upon one's
lead after one has got tired of walking upon one's feet, or
t3 transform one's work-a-day face by painting it over;
but, just because the scientific manner of knowing does not
tatisfy the whole demand of intelligence, philosophy must
supplement it by another manner of knowing." ^
The result then may be briefly expressed thus. Kant
and his successors showed the relativity of the object of
knowledge to the knowing.^ mind. He thus pointed. out
that the ordinary consciousness, and even science, are
abstract and imperfect modes of knowing, in so far as in
their determination of objects they take no account of a
factor which is always present, to wit, the knowing subject.
For tlieir purposes, indeed, this abstraction is justifiable
and necessary, for by it they are enabled witliin their pre-
scribed limits to give a more complete view of these objects
m their relation to each other than if the attempt had
been made to regard them also in relation to the knowing
subject. At the same time the scientific result so arrived
at is imperfect and incomplete, and it has to be recon-
eidered in the hght of a philosophy which retracts this
provisional abstraction. I'or it must be remembered that
the fact that science looks at things only in their relation
to each other, and not to the knomug mind, narrows the
points of view or categories under which it is able to
regard them, or, in other words, limits the questions which
the mind is able to put to nature. Just because science
does not treat its objects as essentially related to the mind,
it is unable to rise to what Hegel calls the point of view
of reason, or of the "notion"; i.e., it is obliged to treat
objects and their relations merely under a set of categories,
the highest of which are those of causality and reciprocity,
and it is incapable of attaining to the conception of their
organic unity. In other words, it is able to reach only a
synthetic unity of given differences, and it cannot discover a
principle of unity out of which the differences spring and
to which they return. Now philosophy goes beyond science
just because, along with the idea of the relativity of things
to the mind, it brings in the conception of such a unity.
Its highest aim is, therefore, not merely, as Kant still
held, to secure a place for the supersensible beyond the
region of experience, but to reinterpret experience, in the
light of a unity which is presupposed in it, but which
cannot be made conscious or explicit until the relation of
cqjerience to the thinking self is seen,— the unity of all
ithings with each other and with the mind that knows them.
I 2. Relation of MetapJij/sic to Psychology. — It Los already
been shown that the doctrine that the thinking subject is
presupposed in all objects of knowledge — or, in other
words, that existence means existence for a conscious self
— is not to be taken in a psychological sense. The idea
tiftt all science is based on psychology, and that, therefore,
' Ilegel, vii. p. 18.
metaphysic and psychology are identical, cannot be retained'
by any one who has entered into the full meaning of th*
Kantian criticism. It is, however, so natural a misinter-
pretation of it, and it is so much favoured by the letter of
the very book* in which it- was first decisively refuted,
that it will bo useful to point out more directly the fallacy
involved in it, especially as this will place us in a better
position to determine the true relation of the two parts of
philosophy t3iU5 confounded.
The misunderstanding first took a definite form in th«
introduction to Locke's Essay, in which he proposes t»
provide against any undue application of the intellectual
powers of man to problems which are loo high for them,
by first e.xamining and measuring the powers themselves.
Stated in this way, it is obvious that the proposal
involves an absurdity ; for we have nothing to measui»
with, except the very powers that are to be measured. To
see round our knowledge and find its boundary, we must
stand outside of it, and where is such a standing ground to
be found ? We cannot by knowing prescribe limits to
knowledge, or, if we seem to be able to do so, it can only
be because we compare our actual knowledge with som*
idea of knowledge which we presuppose. In this way the
ancient sceptics — and modern ^Titers like Sir W. Haniiltoa
and Mr Spencer who have followed them — turned th»
duality involved in the idea of knowledge against its unity,
and argued that, because we cannot know the object
except as difl'erent from and related to the subject, w»
cannot know it as it is in itself. Obviously in thi
argument it is involved that in true or absolute knowledge
the object must not be distinguished at aU from the subjecJj
— to which the easy answer is that icit/iout such distinc-
tion knowledge wpuld be impossible. The sceptic argu-
ment, therefore, lands us in the unhappy case pictured
in the German proverb : " If water chokes us, what shaU
we drink!" The objeet cannot be known if it it
distinguished from the subject, and it cannot be kno^Tn if
it is not distinguished from the subject. Obviously th»
one objection is as good as the other, and both combined
only show that the idea of knowledge involves distinctioi
as well as unity, and unity as well as distinction. Th»
sceptic insists on one of these characteristics to the exclusioB
of the other, and condemns our actual knowledge becauso
it contains both. In Kant there is undoubtedly some traco
of the same fallacy, in so far as the idea by contrast witk
which he condemns the objects of experience as pheno-
menal is the idea of an abstract identity without any
difierence ; but we have seen that with him this abstract
identity is on the point of passing into an altogether
different idea — the idea of self-consciousness as the type of
knowledge.
It appears, then, that the idea of measuring our powen
before we employ thera rests on a paralogism ; for what i<
really meant is that we abstract one of tho elements of th»
idea of knowledge, and then condemn knowledge for having
other elements in it. It is possible to criticize and con-
demn special conceptions as not conforming to our idea
of knowledge ; but it is not possible to criticize the idea
of knowledge itself ; all we can do is to explain it. It ia
possible to see the limited and h}'pothetical character of
certain of our ideas or explanations of things, because wo
are conscious that in devoJoping them we have left out of
account certain elements necessary to the whole truth ;
but this criticism itself implies, as tho standard to ^vhich we
appeal, a consciousness of truth and reality, a consciousness
which we cannot further criticize. Here, therefore, wo
come upon what must seem to all who think ,it admissiblt
to question the very possibility of knowledge an inevitablo
reasoning in a circle. We can answer objections only bjf,
means of the very idea which they dispute. But tb«
METAPHYSIC
89
Miswer is nerertheless a good one ; for the objector also
stands within the very circle which he seeks to break, and
has no means of breaking it except itself. As soon as he
qjeaks, he can be' refuted by his own words ; for his doubts
also presuppose that unity of the intelligence and the
intelligible world which he pretends to deny.
The error, however, cannot be fully corrected until we
tonsider what gives it plausibility. The confusion of the
metaphysical with the p.sychological problem is due to the
fact that the being who is the subject of knowledge, for
whom all exists that does exist, appears to be one, and only
sne, of the many objects of knowledge. AVTien we say
that existence means only an existence for a thinking self,
we seem to be identifying the whole world \vith the feelings
and ideas of men, i.e., with certain phenomena that belong
to the life of a class of beings which only forms a part of
that world, — phenomena, moreover, that are not exactly
the same in any two of that ckss of beings. If we are to
escape this difficulty it is obvious that we must be able to
ieparate the conscious self or subject, as it is implied in
lil knowledge, from the nature of man as a being who
" though formally self-conscious " is yet " part of tliis par-
tial world," i.e., one of the objects which we know along with
and in distinction from other objects, and in whom " the
«8lf-consciousnes3 which is in itself complete, and which
in its completeness includes the world as its object," is only
progressively realized.* Metaphysichas to deal with con-
ditions of the knowable, and hence with self-consciousness
ks that unity which is implied in all that is and is kno^vn.
Psychology has to inquire how this seLf-consciousnes^ is
nsalized or developed in man, in whom the consciousness
of self grows with the consciousness of a world in space
»nd time, of which he individually is only a part, and to parts
•f which only he stands in immediate relation. In con-
•idering the former question we are considering the sphere
within which all knowledge and all objects of knowledge are
•ontained. In considering the latter we are selecting one
particular object or class of objects within this sphere, —
although no doubt it must make a great difference in our
treatment of this object that we have to consider it as
asisting not only for 'js but for itself. If nature " becomes
self-conscious in man," it is impossible to treat man
taerelt/ as one among the other objects of nature. But it
is not less true that he is one of those objects, and, in this
point of view, the department of science and philosophy
that deals with his life is as distinct from metaphysic —
which deals \vith the conditions of all knowing and being
— as is astronomy or physics. In both cases we h^ive
before us objects which we may consider in themst-zes
•part from their relations to the conscious subject, and
in both cases we must take cognizance of these relations if
wo would have a complete and final view of those objects.
It is possible to have a purely objective anthropology or
psychology — which abstracts from the relation of man to
the mind that knows him — just as it is possible to have a
purely objective science of nature. Such a natural science
•f man, however, will necessarily abstract at the same 'time
from the fact that in man is manifested that universal
principle in relation to which all things are and are kno\rn.
In other words, it will omit that distinctive characteristic of
man's being in virtue of which he is a subject of knowledge
and a moral agent. Hence the abstraction in this case is
more likely to lead to positive error, more Ukely to produce
Bot only an imperfect but a distorted view of the object.
Inorganic nature, if we take it in itse/f, is not untruly
Tiewed, under the categories of causality and reciprocity,
as a collection of objects externally determined by each
<|ther ; the error lies only in taldng it as if it could exist
' Hume, vol. i. p. 131 (Green's edition).
in itself. Even organic beings do not suffer much injustici'
in being brought under such categories : for, though, as
living and still more as sensitive beings, they involve in
themeelves and in their relation to the world a kind of
unity of differences to which the categories of external
relation imperfectly correspond, yet they are not such
nnitics for tkemsel lies, but only for tif. In other words, the
principle through which they are and are known is still
external to tliem. Hence also they are determined by
outward influences, though these influences act rather as
stimuli to what we may call the self-determined movement
of their own life than as mechanical or chemical force*
which change it. But in man, in so far as he is self-con
s'-'ous, — and it is self-consciousness that makes him man,
— the unity through which all things are and are known
is manifested ; and therefore he is emancipated, or at
least is continually emancipating himself, from the law
of external influence. Nature and necessity exist for
him as that from which his life starts, in relation to which
he becomes conscious of himself, against which ho ha.<
to assert himself, and in the complete overcoming of
which hes the end of all his endeavour. Nature is the
negative rather than the positive starting-point of his
existence, the presupposition against which he reacts rather
than that on which he proceeds ; and, therefore, to treat him
simply as a natural being is even more inaccurate and
misleading than to forget or deny his relation to nature
altogether. A true psychology must, however, avoid both
errors ; it must conceive man as at once spiritual and natural ;
it must find a reconciliation of freedom and necessity. It
must face all the difficulties involved in the conception
of the absolute principle of self-consciousness, — through
which all things are and are known, — as manifesting itself
in the life of a being like man, who " comes to himself "
only by a long process of development out of the uncon-.
sciousness of a merely animal existence.
This problem first presented itself in a distinct form in
the discussions of the Socratic school as to the nature of
knowledge, discusisions which turn mainly upon the relation
of the conscious to the unconscious element in thought.
Socrates, by his method more than by any direct state-
ment, drew attention to the fact that all particular judg-
ments in morals involve or presuppose a universal principle.
At the same time he pointed out that, so far from this
universal principle being known to those who are con-
tinually making such judgments, th-ey are not even
conscious of its existence. They constantly use general
terms whose meaning they have never even thought of
defining. The beginning of a rational lifefor them must
therefore lie in their becoming conscious of their ignorance,
i.e., conscious that they have beer all along judging, and
therefore acting, on untested and even unkno^vn assump-
tions. They must bring the unconscious universal to the
light of day and define it, for until that i.^ done It is
impossible to live a moral, that is, a rational life. " Virtue
is knowledge," i.e., it is acting, not according to opinions,
or particidar judgments, — whose universal is unknown, and
which therefore may be regarded as expressing merely the
impulses or habits of the individual, — but ip view of a
universal principle determined by reason.
The onesidednesrs of this view- — which absolutely con-
demns as vice all virtue that is not based on conscious
principle — was partly corrected by another part of the
doctrine of Socrates, who taught that knowledge is some-
thing that must be evolved from within the mind, and not
merely communicated to it from without. For this impUes
that the moral principle may be present in men's minds,
and may rule their thoughts and actions, long before
they become directly conscious of it. They are rational
although they have never thought about reason, and tliey
90
M E T A P H Y S I C
do not wait for acientiSo ethics to judge and act morally,
any more than they wait for logic to reason correctly. It
is this line of thought which 13 universali2ed and mythically
expressed by Plato in his doctrine of "reminiscence."
According to this myth, we were conscious of ideas or
universals in our pre-natal state ; we forgot them in the
shock of birth into this mortal life; but in feeling or
sharing the rapture of the poet or the lover we recall them
03 identified or confused with individual objects which
;" are like them, or partake in them." The same explana-
tion is given of the practical skill of the general and the
statesman, and even of tlie " right opinion " which guides
the ordinary good man. Such opinion is neither knowledge
nor ignorance : not knowledge, for general principles or
ideas are not in it present to the mind as ideas, and there-
fore the particular cannot be distinctly subsumed under
them ; yet not ignorance, for the ideas are after all present,
though wrapped up in the particulars or confused with
them. Nay, in the Theideim, Plato endeavours to show
that the pure particular without the universal, sensations
without ideas, cannot enter into our consciousness at all,
and that therefore the lowest point to which a conscious
being can descend is " opinion," in which particular and
universal, sensible and intelligible, are mingled together.
In other words, no conscious being can apprehend the
particular except through the universal, though that uni-
versal may be present only in consciousness and not to
it. The task of philosophy is therefore only to make men
"recollect themselves," i.e., to make self-conscious that
universality of thought in which all rational beings
"partake,"' or which, in the language of later philosophy,
constitutes reason. The imperfection pf Plato's view lay,
however, in this, that, while he clearly recognized that the
condition of all consciousneus of the particular is the
universal, he did not see with equal clearness that the
universal has a meaning only in relation to the particular.
And this tendency to separate universal from particular is
naturally accompanied by a tendency to set the subjective
against the objective, and to regard the world, not as the
mapifestation of reason, but as a daalistic world, in which
reason is chained to a lower principle — a world which
can at best only give a hint or suggestion to the mind to
enable it to recollect itself and recover for itSelf its own
treasures. Thus the false method of introspection, the
" high priori road " of mysticism, was at least opened up
by Plato, if he did not altogether forsake the narrower
and harder way to the spiritual world through nature and
experience.
The great step m advance taken by Aristotle was due to
his seeing the danger of this tendency. Those, however,
T.'ho have maintained that Ai'isfotle is the great a posteriori
philosopher,' — as Plato is the great a priori philosopher, —
have entirely mistaken the bearing of Aristotle's criticism
of the Platonic theory. As strongly as Plato does Aristotle
maintain that reason is SwdVet mvTa ra vorjrd, and that,
therefore, the apprehension of truth br/ the mind is not a
mere external communication of it to the mind, but rather
is the mind coming to a consciousness of itself. As firmly
as Plato does he declare thai truth in its highest form is
self-evidencing, i.e., that the principles of science, the laws
of nature, when once they have been discovered, are seen
to be true by their own light. His statements to this
eifect have been neglected or explained away, because
they were supposed to be inconsistent with his still more
frequently reiterated assertions that it is only from
experience and by induction that the truth of things can
be discovered. Writers of a later day, — who came to
Aristotle with an idea of a fixed opposition between a
priori and a posteriori, and who held that the only possible
alternatives were either to divide knowledge between the
two or to explain away one of (hem, — coula not coraprebead
that Aristotle might be in earnest both in asserting that
knowledge is derived from experience aTid.in asserting thut
it is an apprehension by reason of that which is identical
with itself and needs no extraneous evidence. Bn^
Aristotle started with no such fixed opposition. On the
contrary, any one who reads the last chapter of tha
Posterior Analytics will see that he had no difficulty iii
maintaining that knowledge begins in the apprehension of
TO Kaff cKacTTov in sense perception, and that it proceeds
from many perceptions to experience, and from many
experiences to science ; while at the same time he declared
that the principles of science have their evidence in tliemJ
selves. And the meaning of this declaration is 6ho\ra ia'
the Pe Anima, where we find him speaking of knowledge as
the realization in the " passive reason " of man of an " active
reason " which is eternal and unchangeable, and which ia'
the consciousness of itself includes the knowledge of all
things. Of this realization, indeed, there is in man only
the potentiality or capacity, but just because this is a pur«
or universal capacity, because, as Aristotle puts it, it has no
quality or determination of its own to stand between it and
its objects, it is a capacity in v.hich the absolute reason can
reahze itself, a capacity of knowing all things. Here we
have Plato's myth of reminiscence freed from the metaphor
of memory, and reduced to scientific terms ; for that myth
simply meant that the evolution of knowledge is th«
development of the mind to the consciousness of itself, and
of all that is potentially in it. Only, by the combination
of this doctrine with the idea of the necessity of induction,
Aristotle at the same time guards against the pureljr
subjective interpretation to which in Plato it was liable^
For the process by v/hich the mind " comes to itself '.' is
conceived as a process by which at the same time it rises
from the particular to the universal, from the yvwpi/ia
rj/xiv to the yyiipi/ia ajrXws, from the bare apprehension of
the facts of experience to the knowledge of them througfc
their principles or lav/s.
Yet Aristotle was as little able as Plato to work out fully
a theory of the relation between the universal and th
individr.r.1 reason ; and the cause of this failure was Ia
both cases substantially the same. In Plato's philosophy,
the ideal tended to divorce itself from the phenomenal
world in such wiso that the latter was regarded only as
suggesting or partaking in the former, but not as entirely
explicable by it. It was not merely that, to the mind of the
individual in its progress, the veil was only gradually lifted
from the rationality of the world, but that in the world
there was an irrational element from which the mind
could save itself only by flight into the region of abstrac-
tion. And, though Aristotle by his doctrine of. the essentia!
relation of ideas to experience, or of the development of
the mind to the acquisition of knowledge of the world,
seemed to be on the way to correct this error, yet he too
shrinks from regarding the pjienomenal world as in itself
intelligible. To him also an irrational matter mingles with
things, and is in them a source of contingency and imper-
fection. Chance is not merely the reflexion upon the world
of our imperfect knowledge, but a fact of experience, and
there is therefore a region in which our best science cannot
rise above generality to universality. In this way thers
remains for Aristotle an absolute a posteriori, a reality which
cannot bo understood, and which we can scarcely conceivs
as existing at all for the divine intelligence. At this point
the Aristotelian philosophy appears to stand between two
alternatives, either that, in the sense of pantheism, the fintt*
world and its contingency is an illusion, or that it is con-
tingent only for the growing intelligence of man, which
fully understands neither itself nor the world which is its
object. Aristotle, however, docs not choose either horn ol
METAPHYSIC
91
the dilemma, and leaves ub therefore with an unresolved
dualism between thought and its object ; and this again
necessarily involves a dualispa between the active reason,
which, as he asserts, realizes itself in man, and the passive
reason which constitutes his nature as a finite being.
In the Middle Ages the Platonic and Aristotelian idea
fliat the apprehension of objective truth is one with the
evolution of the mind to self-consciousness seemed to be
entirely lost. Knowledge of the finite world. was regarded
as ind&erent, and knowledge of the infinite was conceived
to be something given on authority, and in reference to
which the mind was confined to an attitude of passive
reception or implicit faith. No greater slavery of the
spirit can be conceived than that in which even the
truths of religion and morality — the truths that regard the
inmost life of the spirit itself — were takeu as a lesson
to be learned by rote from the lips of a teacher. Yet
the consciousness that such truth, if it was to be received
by the mind, still more if it was to transform the mind,
could not be entirely foreign to it, found a voice in the
scholastic philosophy. And the compromise or truce
between faith and reason expressed in the saying of Anselm
credo ut intelligapi, — according to which reason was to
confine itself to the analysis and demonstration of the data
received in implicit faith from the church, — prepared the
way for the recognition that the two are not essentially
at variance. The mind tfcat proceeds from veneratio to
dehclado, from awe and submission to the doctrine to
enjoyment and appreciation of it, must already in its awe
and submission have the beginnings of an intelligent
appreciation. Anselm's saying might be understood simply
as meaning that we must have spiritual experience ere
we can understand the things of the spirit. And in this
sense it was adopted by the Reformers to express an idea
almost the opposite of that with which the scholastics
had associated it, — the idea that the direct apprehension of
spiritual truth as entering into the inner life of the subject,
as identified with his very consciousness of self, is the basis
of all knowledge of it. In the Protestant church of the
period after the Reformation, we find a growing tendency
to insist on the subjectivity of religion, in the same exclusive
and one-sided way iu which the mediaeval church had
insisted on its objectivity. In some extreme representa-
tives of Protestantism this went so far as to lead to a
disregard, almost to a rejection, of all objective doctrine,
and a reduction of theology to an account of the religious
consciousness. On the other hand, Tyhile religion was thus
made subjective, science claimed to be purely objective,
and the followers of Bacon seemed to adopt towards nature
the same attitude of passive receptivity which the mediaeval
Christian was taught to hold towards the church. WTiile
man was to learn everything from himself in religion, he
was to learn nothing from himiself in science. His aim
must be to exclude subjective idola, in other words, to
accept the facts as they were given, and keep himself out of
ihe way. The inevitable result of this difference of view
as to the nature of knowledge in these two different
regions was, however, on the one hand a withdrawal of
religion from all connexion with finite interests, and,
especially from the attempt to connect religious principles
with the knowledge of the finite world, and, on the other
hand, an increasing tendency in those who represented
£nite science to regard religion as something merely
subjective and even individual, as a feeling which could
not be translated into thought or made the basis of any
knowledge of the objective world.
The opposite principles of certitude which were thus
, «et up for religious truth and truth of science need only
.to be brought together and contrasted to betray that they
Jest upon opposite abstractions, neither of v/hich expresses
the complete nature of truth or knowledge. On tho onj
hand the truths of religion were maintained just because
they were not, or v.-ere not merely, objective,' but. were
capable of being tested by inner experience, and identified
with the self-consciousness of the individual On the other
hand the truths of science were maintained because they
were not, or were not merely, subjective, but were capable
of being verified in objective experience. It was rightly
seen oa the one side +hat mere subjective feelings or
opinions have no validity for any one but the subject of
them, and on the other side that what is merely objective
or externally given can have permanent value and interest
for the intelligence only as it ceases to be mere isolated
and unrelated fact — nay, that, even when science has
discovered law and order in nature, it still wants the
highest value and interest so long as that law and order are
not seen as standing in essential relation to the intelligence
itself. The idea of truth or knowledge as that which is at
once objective and subjective, as the unity of things T,-ith the
mind that knows them, enables us fo understand the con-
demuation which the religious mind passed upon a merely
external dogma, and even its lack of interest in a science
which presented itself as an account of merely objective or
external facts. And it enables us also to understand the
way in which scientific men insisted upon objective fact
as the basis of all knowledge, and the disrespect which
they felt for a religion which seemed to admit that it had
no such support. ^¥hat is wanted to clear up the confusion
on both sides is the growth of the perception among
Bcientifio men that the objectivity which they are seeking
cannot be mere objectivity (which would be unmeaning),
but an objectivity that stands in essential relation 'to the
inteOigence, and, on the other hand, the growth of the
perception among religious men that the subjectivity of
religion only means that God, who is the objective principle
by whom things are, and are known, is spiritual, and can
therefore be revealed to the spirit. When these two cor-
rections have been made, it must become obvious that the
religious consciousness is not the consciousness of another
object than that which is present in finite experience and
science, but simply a higher way of knowing the same
-object. And in this it is also involved that the two ideas
of a priori and a posteriori, of that which is evolved from
within and that which is given from without, are not
essentially opposed to each other, but that the o posteriori
is simply the first form of a consciousness which in its
ultimate development must become a priori.
In that philosophy of compromise which was initiated
by Descartes, onepart of knowledge was regarded as innate,
or developed from within, and another part as empirical,
or imparted from without. .In the second period of the
history of modern philosophy this compromise was broken,
and the names of Locke and Leibnitz — though with some
hesitation on both sides — represent respectively the theories
that all knowledge is a posteriori and that all knowledge
' is a priori. The compromise seemed to be renewed with
Kant, but the form in which it was renewed pointed, as
has been already shown, to something more than a com-
promise, for his doctrine was that the a posteriori element,
the facts, exist for us only under a priori conditions, or,
in other words, that what is usually called a posteriori
is in part a priori. The criticism of this view need not
be repeated. It is sufficient here to say that if, as Kant
shows, the elements are inseparable or organically united,
it is impossible to allege that so much belongs to the one
and so much to the other. Furthermore, the consciousmiss
of an essential difference in the elements of knowledge is
possible only so far as that difference is transcended by the
unity of knowledge. We can distinguish the o priori from
the a posteriori only on condition that we can transcen4
92
M E T A P H Y S I 0'
the distinction, and this means that the distinction itself
is not absolute, but that there is a point of view from
which the a posteriori may be regarded as a priori, and
that which is given from mthout to the spirit may be
referred to its own self-determined development.
Now it is just here that we come upon the turning-point
of the philosophical controversy, in the form which it has
taken in modern times. The problem may be expressed
thus — In what sense can we apply the idea of development
to the human spirit ? Are we to tref.t that development
as merely a determination from without, or as an evolution
from within, or as partly the one and partly the other ?
In a sense all writers of the present day would admit that
this last is the case. For, on the one hand, even the
Darwinian theory accounts for development by aid of
what we may call the a priori tendency of the individual
to maintain itself in the struggle for existence, though it
supposes that the condition or medium in which the indi-
ividual is placed determines the direction in which that
'development proceeds. And, on the other hand, no one
.now would adopt the Leibnltzian theory that the indi-
vidual is a monad, whose self-development is entirely con-
ditioned by itself in such a sense that all the relations
iwiiich it has to other existences are merely apparent, and
that the coincidence of its life with the lite of the world is
the result of a pre-established harmony. On both sides,
therefore, the idea of self-determmatiou would be admitted,
though the tendency of the Darwinians would be to regard
this self-determination as something merely formal ; and
on both sides it would also be admitted that the self-
determination does not exclude a determination from with-
out, though extreme opponents of Darwin might be inclined
,to reduce this determination to a mere stimulus or external
condition of the development of the nature of the subject
to which the stimulus i.s applied. The question, however,
remains whether, after all, this opposition of without and
within is an absolute one, or whether there is any point of
view from which it may be transcended. To Aristotle it
seemed possible to answer this question in the afiirmative,
because he conceived that the reason of man is a pure or
universal Swo/iit, the evolution of which to complete self-
consciousness is one with the process whereby the objective
world comes to be known. Yet, as Aristotle admitted the
existence in the world of a material principle which was
essentially different from the ideal principle of reason, he
was obliged to limit his statement as to the possible unity
of the subjective and the objective consciousness, and to
say merely that " in things vnthout matter the knower is
identical with the known." But this would immediately
lead to the conclusion that the pure development of reason
must be secured by abstraction from all finite and material
objects, rather than by a thorough comprehension of them.
The freedom of the spirit, on this theory, must be a negative
and not a positive freedom, a freedom won, not by over-
coming the world, but by withdrawing ourselves from its
influence. It remained, therefore, for modern philosophy
to work out the Aristotelian idea that the rational being
as such, in spite of its necessary relation to and depend-
ence on an external world, is never in an absolute sense
externally determined. And, as wo have already seen, the
Kantian philosophy brought this problem within the reach
of solution, in so far as it showed, first, that objective
existence can have no meaning except existence for a
thinking self, and, secondly, that existence for a thinking
self means existence the consciousness of which is " capable
of being combined with the consciousness of self." Add
further to these propositions what was shown by Kant's
successors, that that only can be combined with the con-
sciousness of self which is essentially related to it, and wo
Snrive at an idealistic theory of the world, which enables
us at once to underEtan'''i the relative value of the distinct
tion between self-determination and determination from
without, and at the same time to see that its value is onlj
relative. If it be true that nothing exists which is not a
possible object of consciousness, and again that there is no
possible object of consciousness which is not essentially
rek'ted to self-consciousnes.s, then the phenomena of tli'o
external world, which at first present themselves under tlie
aspect of contingent facts, must be capable of being ulti-
mately recognized as the manifestation of reason ; and the
history of the conscious being in his relations with that
world is net a struggle between two independent and
unrelated forces, but the evolution by antagonism of one
spiritual principle. It is, on this view, the same life which,
within us is striving for development, and which without)
us conditions that development. And the reason why the
two term.s, the self and the not-self, thus appear to boi
independent of each other, or to be brought together only]
as they externally act or react upon each other, lies in this,
that the object is imperfectly known, and the subject ia
imperfectly self-conscious. This, however, does not make it
less true that in self-consciousness is to be found the prin-
ciple in reference to which the whole process may be
explained, and therefore that the self-conscious subject, as
such, lives a life which belongs to him, not merely as one
object among others, but as having in himself the principle
from which the life and being of all proceeds.
From this point of view, as has been already indicated,'
the relative value of a theory of human development, such
as that which might be based on the ideas of Darwin,
would not be denied. The conscious being may be regarded
simply as an externally determined object, and the incorrectr
ness of this assumption will not entirely destroy the value
of the results attained, especially if, as is often the case
with those who seek to construct a natural science of man,
the assimiption itself is not very strictly adhered to, but
corrected by the tacit admission of other conceptions some-
what inconsistent with it. But, at the same time, it woulfl
require to be pointed out that such a science is necessarily
abstract and imperfect, as it omits from its view the
central fact in the life of the object of which it treats. It
can do nothing to account for man's consciousness, or his
capacity of becoming conscious, of the influences by which
he is supposed to be determined , or, to put it from the
other side, it takes for granted that the objects that
influence man are intelligible objects, "capable of being
combined with the consciousness of self," without seeing,
how much is involved in this assumption. Now it is
evident that the consciousness of an influonce cannot bo
explained by the influence itself, nor even by that taken
together with the nature of the sensitive beings subjected
to it. It is evident also that an influence mediated by
consciousness is not, strictly speaking, an external influonce,
but that it is already transformed, and in jirocess of being
further transformed, by the development of the self to
which it is present. For the dawn of consciousness, in
which the external object first comes into existence for us
as opposed to the self, is at the same time the beginning
of the process by which its externality is negated or over,
come. Self-consciousness is that which makes us indi--
viduals in_a sense in which individuality can be predicated
of none but a self-conscious being. For, in determinina
himself as a self, the individual at the same time exclude^
from himself every other thing and being, and detcrminea
them as external objects. lie emancipates himself from
the world at the same time that he repels the world from'
himself. Yet this movement of thought, by which hw
individuality is constituted, is also that by which he is liftedj
above mere individuality, for, in becoming conscious of sell
and not-self in their opposition and relation, he ceases tQ
METAPHYSIC
93
be simply identified with the one to the exclusion of the
other. His finite individutility is regarded by him from a
universal point of- view, in which it has no less and no more
importance than any other individuality, or in which its
greater or less importance is determined only by its place
in the whole. On this universality of consciousness rests
the possibility of science and of morality. For all science
is just a contemplation of the world in ordir.e ad univfrsum
and not in ordine ad individuum ; and all morality is just
action with a view to an interest which belongs to the
agent, not as this individual, but as a member of a greater
whole, and ultimately of the absolute whole in which all
men and all things are included.
In this nature of the conscious subject lies also the
possibility of metaphysic in the sense of Aristotle, as that
science which goes back to a vpCrrov <j>v<TeL, a beginning
which is prior to the existence in consciousness of the
individual self, and onward to an end in which the divisions
of the finite consciousness are transcended, — as including,
in short, ontology, or metaphysic in the narrower sense, on
the one side, and theology, or the philosophy of religion,
on the other. In truth, these two extremes of science are
necessarily bound together : we can only go back to the
beginning if we can go on to the end ; we can only recover
the first unity if we can anticipate the last. Or, to free
the subject more definitely from the associations of time,
we cannot apprehend the unity which is involved or pre-
supposed in all the differences of our conscious life except
in so far as we can look at our individual existence from
the point of view of the whole to which it belongs. This
will become evident if we consider the nature of the limits
which have to be transcended by such a science. The
individual conscious subject, as he finds himself at first,
is but one being in a world that stretches out, apparently
without limits, on every side of him. Of the things by
which he is immediately surrounded he sees but a small
part, and the influences which he receives from them are,
as he knows, like the wave that breaks upon a shore from
an unknown ocean, only the last partial expression of
impulses that come from regions beyond his ken. Again,
he finds himself as one in a changing series of beings, of
which he knows only the last preceding terms, and he is
aware that in a few years he, as one of this series, will
cease to be. He is thus to himself a definitely limited
being, and though his knowledge of himself and his world
may be gradually widened so as to reach- some little way
back into the past, and anticipate a little of the future, or
may go outwards in space to embrace a widening circle of
existences around him, yet he always stops at a limit, of
which he is conscious that it is no absolute limit, but
simply an arbitrary halting-place where vision grows
indistinct and imperfect. When he reflects upon himself
from this point of view, he is forced to regard himself as
but a fragment, and a fragment of an unknown whole, by
which his whole being is determined to be what it is.
His highest knowledge seems to be but a consciousness
of his ignorance, his highest freedom a determination by
motives the ultimate meaning of which is hid -from him.
So far there seems to be no room for any metaphysical
knowledge, -any knowledge of ourselves and our world
which is other than relative and in ordiru ad individuum.
But further reflexion shows that in this very consciousness
of limit there is implied a consciousness of that which is
beyond limit. While we proceed from part to part, beginning
with ourselves and our immediate surroundings, and follow-
ing out lines of connexion that lose themselves in the dis-
tance, we< are guided by a consciousness of the whole as a
4inity through which the parts are determined. Nay, it is
just the presence of this consciousness that makes us capable
of what seems the piecework of our knowledge, in which,
by the aid of the principle of causality, we connect parti-
cular with particular, and so gradually extend the sphere
of light into the encompassing darkness. For that
principle simply means that the limited external object
does not suflSciently explain to us its own existence, and
that therefore we are forced to explain it by a reference to
something beyond it. It means, in other words, that wa
cannot rest in that which is not a self-bounded, self-
determined whole. The application of the category of
external determination has therefore an essential reference
to the higher category of self-determination. The mere
endlessness of space and time has no meaning except in
opposition, yet in relation, to the true infinity of which
we find the type in self-conscious thought Or, to put it
in the Kantian form in which it is already familiar to us,
the consciousness of the objective world in space and time
stands in essential relation to the unity of self-conscious-
ness. And if when we regard the former exclusively we
are forced to view ourselves as insignificant and diort-
sighted finite beings in an infinite universe, when we
regard the latter we are enabled to see that in all this
universe there is revealed only that spiritual principle
which we find also in ourselves. In this way a new light
is thrown on our first consciousness of ignorance. The
strivings of our reason after knowledge can no longerbe
regarded as strivings after an unknown goal, but rather
after a goal which it has prescribed for itself. The narrow
limits of our individual life are not removed, but they
cease to be for us the limits of a narrow circle of definition
within a formless infinite. They become the limits of a
sphere within a sphere, a sphere which is defined by the
idea of knowledge or self-consciousness itself, and in which
therefore, however we may wander, we are every\vhere at
home. In religious language, the sphere is not a mere
universe, but God, who is without us only as He is within
us, so that "by the God within wo can understand the
God without."
Again, as. this consciousness takes man beyond his
immediate existence, and enables him to determine it in
relation to an absolute unity of all things in God, so it
enables him to go back to a unity which is behind or
prior to that existence. For, if the individual can look at
himself as he looks at others, and at others as he looks at
himself, i.e., from a point of view which is unaffected by
his individuality, and in which that individuality is for him
only what it is for impartial reason, he can have nothjng in
him which binds his consciousness to hia individuality ail
mere individuality ; as therefore he can go beyond himself
to apprehend the whole in which his individuality has a
place, there is nothing to prevent him from going back
upon himself, and upon' the conditions which are prior to
his own individual being. H^ is not tied to his immediate
life, and can go below it just as he can rise above it.
" O God, I think Thy thoughts after Thee," said Kepler.
In reading the " thoughts " written in the planetary
system, Kepler was discovering the meaning of that
which is simpler and more elementary than the existence
of man, as a cycle of mechanical relations are simpler apd
more elementary than self-consciousness. Yet it was a
true feeling that led him to connect this descent into the
mechanical world with God. For it is only in virtue of
the same faculty which enables us to rise to the absolute
life which includes and subordinates our own that we can
so free us from the image of cur own conscious life as to
apprehend and fix in thought the simpler relations of
purely physical existence. But the same faculty of going
back upon ourselves has a still deeper manifestation.
Not only can we abstract from ourselves so as to under-
stand the inorganic world, we can also abstract from oup-
selves so as to understand the conditions which are prior
94
.METAPJBYSIC
to the tHought, and therefore to the existence, of any
.objective external world at all, the universal conditions of
the knowablo and therefore also, of reality. In doing so,
to use Hegel's metaphor, which is but an extension of
Kepler's, we are "thinking what God thought and was
hefore the creation of the world," i.e., wo arc thinking the
spiritual unity presuppossd in all knoiB ledge, and therefore
in all objects of knowledge^the consciousness in relation
to which everything is, and is known.
A, T/ie Rdation of Logic io Melaphysic. — The ordinary
view of logic is based on two presuppositions which tend to
separate it almost entirely from metaphysic : it is based on
the presupposition of an opposition, or at least a merely
external relation, between thought and its object, and again
of an opposition, or merely external relation, between the
form or method and the content or matter of thought. The
intelligence is regarded as dealing with an object which is
given to it externally, and to which, therefore, it can be
true only if it leaves it unchanged and introduces into it
nothing of its own. Trnth, to use a well-known definition,
is the agreement of our conceptions with their objects, and
in bringing about this agreement all the concessions must
be on the side of thought. Conformably to this view, the
processes of thought must be purely analytic; i.e., thought
may break up the given idea of the object into its con-
stituent elements, and again out of these elements it may
recompose the idea in its unity, but it can add nothing and
■take nothing away. It is like an instrument which
alternately dissects a solid mass into smaller parts and
again mechanically presses them together, but which
never penetrates and dissolves the hard matter, still less
fuses it into a new form by bringing it into contact with
new chemical elements.
This conception, like much of the philosophy of which
it is a specimen, is a kind of exaggerated .caricature of one
aspect of the philosophy of Aristotle. Aristotle is the
great analytic philosopher. He first laid down boundaries
in that continuous domain of science which Plato had first
surveyed. Not that he ever completely lost sight of the
unity or continuity of the different sciences which he thus
distinguished. His unrivalled speculative genius is shown
nowhere more clearlythanin those not unfrequent utterances
of speculative insight into the unity of things different, by
which, as at a stroke, he makes his own landmarks and aU
landmarks to disappear. Yfet such utterances generally
stand by themselves, and do not alter the general analytic
spirit of his philosophy. They are not so developed as to
show distinctly the merely relative character of the divisions
and distinctions which are set up, or the limits of the sphere
within which they hold good. Hence it was easy for
minds which pos.sessed something of Ai'istotle's keenness
of understanding without his speculative depth to neglect
such expres.sions, or to explain them away. And this
process of degradation was the more rapid as the philosophy
of Aristotle soon ceased to be studied in his own writings,
and became a traditionary possession of the schools. In
this way we may partly explain how logic came to be
regarded by modiaoval philosophy as a form of thought
which could be altogether separated from the matter, and
by the application of which that matter could be in no way
affected or changed. But for such a view, indeed, it is
difficult to conceive how the schoolmen could have ventured
to apply any logical procc2.sc3 at all to the sacred matter of
dograra. The idea of externally adding anything to the
faith once delivered to the saints was excluded by the
principle of authority ; and the idea of developing out of
that faith anything that was not immediately contained in
it had not yet presented itself to any one. Hence the
business of thought seemed to be purely formal and
analytic, and it was only on the plea of its being such that
its activity could be tolerated at all Nor was this view,
of logic at once changed by the revolt against scholasticism.'
The first philosophical exponents of the modem scientific
movement, while they rejected the matter of dogma as
fictitious, or at least as transcending the sjAere of positive
knowledge, and while they substituted in its place, as the
oljcct of investigation, the facts of exiierience, did not
realize any more than the schoolmen that the form and
method of knowledge could be other than analytic of given
matter. Bacon, their protagoni-st, was above all solicitous
to guard against any subjective aji/icjpa^j'o nalurw, nor did.
lie see that the questions which, in his theory of forms,'
he proposed that science should ask of nature themselves
involved any preconceived theory regarding it. Conscious,
as every true scientific man must be, that the study of
nature involves a constant self-abnegation, a patient self-
distrustful coiu-se of experiment and observation, he an I
his followers did not realize the presuppositions that mak •
the inquiry possible, and by which it must be guided. Still
less did they recognize that the separation between the
mind and its object which they took for granted can only
be a relative division, i.e., a division on the basis of a
unity, and that therefore the self-abnegation of the mind
in its investigation of facts cannot be an absolute self-
abnegation, but is only the first step on the way to the
discovery that the facts are intelligible, and so essentially
related to the intelligence. Hence to them logic still
seemed a mere analytic process, the end and aim of which
was understood to be that a world, existing in itself out
of relation to thought, should be reproduced in a more or
less imperfect imaf in thought. And, when it came to be
suspected bj' a less naive philosopliy of experience that,
after all, certain presuppositions, not givenr in experience
itself, were involved in the scientific interpretation of it,
various expedients were devised to reduce these presupposi-
tions in an indirect way to empirical truths, — expedients
of which Jlill's attempt to base the law of causality upon
an indnctio per enumerationem simpliceni may be taken aa
the type.
when we go back to Aristotle, — who was the "founder
of logic " in the sense that he was the first who treated
logical method as a separate branch of science, — we find
that his division of logic from metaphysic is by no means
so definite and complete as it was made by some of his
successors. The verification of the highest principle of
thought, the law of contradiction, is treated bj- him as the
business of metaphysic. And, though he separates the idea
of truth from the idea of reality, and regards the former
as involving a relation of thought to a reality which is
determined in itself independent of that relation, yet ho
does not regard this independence as by any means absolute.
Truth is defined by him as a connexion or distinction of
ideas which corresponds to a union or separation of things,
but does not necessarily so correspond. This definition,
however, holds good only in so far as things are net
scientifically knowm, or in so far as things not essentially
related are brought together Kara <ri'/j/3c^i;Ko'9. Where
necessity cOraes in, and is apprehended by reason, the
case is different. For in that case we have not merely
an external synthesis, but an essential identity, i.e., a unity
of elements which can neither be, nor be known, apart
from each other. ■ In relation to the principles of science,
therefore, Aristotle holds that error, i.e., a connexion of
ideas not corresponding to a connexion of things, is impos
sible, and that the only alternatives arc knowledge and ig
norance. Either we possess the idea or we do not possess it;
as Aristotle otherwise expresses it, in thought we are either
in contact with the things or not m contact with them;
there is no third possibility. The meaning ef Aristotln
becomes dearer when we remember that, according to hia
JM-E XAT. H Y S I.C
95
\ !e-w, the intelligence, in apprehending the indivisible unity
af elements in the object, is at the same time apprehending
the unity of the object with itself. The mind cannot be
deceived in regard to that which forms a part of its con-
sciousness of itself. In freeing the essential conception of
the object from the contingency of matter, science has
freed the object from that which made it foreign to
intelligence, aad thfe relation of thought to things ceases
to be one if correspondence, and becomes one of identity.
: The legitimate inference from this view of the relation
of the intelligence to the intelligible wor-ld would seem
to be that the partial separation of thought from its object
and its imperfect correspondence with it is characteristic
of our first empirical consciousness of things, and of the
progress from that consciousness to science, but that in
completed science the division ceases. The esse of things
^ not their percipi but their inteUvjx. But, if this be
fe.kec as the trutli, then u'cax no longer be sujiposed that
the process by which scientific knowledge is attained con-
sists simply in an anafysis of the object as it is given in
immediate perception. On the contrary, it must be held
that, if our thought has to submit itself to the object, and
to be brought into conformity with it, by a process of
induction, it is equally true that in thjs process the object
also must be changed, that it may be brought into con-
formity with the princrjjle of thought. The genesis, of
ecience, according to this view, is not merely an analysis
of given facts, but a process of vital transformation by
irhich consciousness on the one side and the object on
the other are brought into unity with each other. The
idea, indeed, of an empty process, a process in which the
activity of the mind is merely formal, is one which will
cot st^ind the slightest examination. A mind without
categories, if auch a thing were conceivable, would have
no questions to ask in relation to the object presented to
it, and could therefore get no answers. Those who make
a pretence of approaching a subject in an absolutely
receptive attitude, and without any presuppositions, only
show that they are unconscious of the categories by
which their thought is ruled ; and they will be most
slavishly guided by these categories just because they
aie unconscious of them. The schoolmen, when
they applied their logical principles to the matter of
Christian dogma, did not recognize that they were doing
more than analysing and bringing out clearly the meaning
of that dogma. But the effect of their work was to turn
the system of divinity into a collection of insoluble puzzles;
for the doctrine was a doctrine of reconciliation between
divine and human, infinite and finite, universal and
particular, and the principle of their method was to treat
all these oppositions as absolute. In like manner it might
be shown that the analysis of social phenomena which was
made in the last century was inadequate and superficial,
just because of the latent assumption of individualism on
which it proceeded, and that the greater success of writers
like Comte and Spencer does not arise merely or mainly
from their being more careful observers of the phenomena
of social life, but in great part from the fact that, rather by
the unconscious movement of opinion than by any distinct
metaphysic, their minds have become possessed bv more
adequate categories.
The idea that the process of thought is mereiy formal,
3r analytic of given matter, is, however, an error that has
t truth underlying it. This is the truth expressed by
Aristotle in his much misunderstood comparison of the
itelligence of man to a tabula rasa, upon which nothing
t first is wTitten,,and again in his assertion — already
noted — that the mind is a pure Si.W//i9, without any
listinguishing quality of its own which could prevent it
• #om apprehending the real liature s>t other things. In
other words, self-conscious reason is not a special thing in
the world, but the principle through which all things are,
and areninderstood ; and hence, as regards the distinction of
things from each other, it is in the first instance undeter-
mined and indifferent, and therefore open to be determined
in one way or another, according to the object to which it
is directed. But this simply means that the conscious
subject, as siich, is not bound to his ovtn individuality, but
can regard things, nay, in a sense, must regard them, from
a point of view which is independent of it. This is what
makes possible the self-restraint and self-abnegation pre-,
scribed to the scientific man, whose whole duty, as it is often
said, is to keep himself out of the way and let the objects
speak, to lay aside all subjective idola and prejudices
that stand between him and the reality of things. This at
first sight may seem to be equivalent to the assertion that
the mind ought to be in a state of simple passivity or
receptivity towards objects. What is really meant, how-'
.ever, is not that the intelligence should go out of itself, or
cease to be itself, that it may know its object, but simply
that it should show itself in its universality, or freedom
from the limits of the individual nature. The self-abnega-
tion of science is an endeavour, so to speak, to see the
object with its own eyes, but this it can do only in so far
as the consciousness for which the object is is that con-'
sciousness in relation to which alone aU objects are, and
are understood. Or, to put it in another form, the con-
scious self in its scientific self-abnegation does not give
itself up to another, and become purely passive ; it only
gives up all activity which is not the activity of that
universal thought for which and through which all things
are. Hence, when it has so abnegated itself, its most intense
constructive activity is just beginning, though, just so far
as the self-abnegation has been real, that constructive
activity has become one ■<f!\i)i the self-revelation of the
object. As, however, it is only through the constructive
activity of thought that there exists for us any object at
all, so it is only through its continued activity that the
conception of the object is changed, till it is completely,
revealed and known. And this activity involves a con-
tinuous synthesis, by which" an ever wider range of facts
is brought together in an ever more definite unity, until
the mind has, if we may use the expression, exhausted its
store' of categories upon the world, and until the world has
completely revealed itself in its unity with itself and with'
the mind. ,
To combine these two ideas — on the one hand that science
begins in a self-abnegation by which the mind renounces
all subjective prejudices, and thereby attains a purely
objective attitude, and on the other hand that this purely
objective attitude is not a mere attitude of reception, birt
one in which the mind is continually transforming the'
object by its own categories, — to see that the universality
of the mind in knowing is not mere emptiness, and that its
activity is synthetic just when it is most free ftom all pre-
suppositions extraneous to the nature of its object, — is one
of the greatest difficulties of the student of metaphysic'
Universality at first looks so like emptiness, and a universal
activity so like a merely formal activity, that it is no
wonder that the one should be mistaken for the other.;
But if we make such a confusion, we may soon be forced
to choose between a sensationalism that makes knowledge
impossible and a mysticism which makes it empty. The
pure identity of thought with itself which is involved in
the process of analysis is put on the one side, aJid the
manifold matter of experience which is the object of
thought on the other, and between these opposites no
mediation is possible. If we take our stand upon the
latter, we are forced to reject all mental synthesis as
invalid, because it involves a subjective addition to ths
96
31 E T A P H Y S I C
facts : if we tal^e cur stand on tlio former, we are com-
pelled to rejard all nljjcctive experience as iiTational.
l)ei;au<s it doc? not correspond to thu pure identity of
ihouj-'ht.
In Aristotle's view of logic it cannot be said that this
•linRenlty i^ clearly solved, though he seems to have seen
the- error of Ijotli extrenies. On the one hand he often
recognizes the synthetic character of the process of induc-
tion, as when lie speaks of the universal idea or law as a
central principle, in which we must find the key to all tha
<lilficulties suggested by different aspects of a given subject.
Yet in other places we trace the inlluence of a merely ana-
lytic conception of that process as a process in which the
universal is to be reached by abstracting from the peculi-
arities of individuals. And this conception of it is favoured
by Aristotle's mctajihysical theory, according to which the
forms of things in the fiuile world are manifested in a
resisting matter, a matter which prevents them from being
perfectly or universally realized. For, in so far as this is
the case, tlie facts will not be entirely explained by the
knowledge of the form, and the knowledge of the form
must be obtained, not by combining all the facts, but rather
by abstracting from them. Again, in Aristotle's account
of the process of thought in the Prior Ana/i/tics, he
regards it as a formal deductive process ; and, though
in the Poslerior Anutijlics he attempts to give a .synthetic
meaning to the syllogism by treating it as the method in
which tliG properties of a thing may be proved of it, or
combined with it, through its essential definition, yet this
adventitious meaning bestowed upon the syllogistic process
does not alter its essential nature. The ultimate source of
this inadequate view of the process of thought seems to lie
in Aristotle's imperfect conception of the unity or identity
which is for him the type of knowledge. For, though, both
in the Metaphysic and the De Anima, he defines that identity
as self-consciousness or as a consciousness of objects which
is identical with self-consciousness, yet he does not seem
slearly to distinguish between a unity in which there is no
difference and a unity in wliich difference is transcended and
reconciled. This seems to bo shown by his description of the
principles which reason apprehends as individua or indi-
visible unities, rather than unities which imply, while they
transcend, difference. Yet, in this definition of the unity
of knowledge as self-consciousness, Aristotle has implicitly
admitted that there is a duality or difference in the unity
itielf, and this might have been exi^ected to modify his
conception of the relation of consciousness to its objects.
For, as self-consciousness is not simple like a chemical
element, but only in tlie sense that it is an indissoluble
unity of opposites, it might have been anticipated that
one who had realized self-consciousness as the principle
of knowledge would bo able to regard the opposition
between the consciousness of self and the consciousness of
the world as itself also capable of being conceived as a
unity.
This misconception of Aristotle may be shown in
another way. In the Metaphysic we find liim lapng down
\vhat is called , the logical law of contradiction as the
ultimate principle of knowledge. The meaning of this
principle, however, as Ai'istotlo states it, is simply that
thought in its essence i.s definition or distinction. If, as
Heraclitus say.s, everything at once is arid is not, if wo
cannot attach any definite predicates to things by which
they may be distinguished from each other, then, as
Aristotle argues, thought is chaos, and knowledge is
impossible. If determination bo not negation, if the
r.Kertion of A bo not the negation of not-A, then there is
no meaning in words. The criticism to be made on this
view is obviously, not that it is a false statement of the law
of thought, but that it is an impsrfoct statement of it.
Thought is undoubtedly distinction ; and, if all distinction'
bo confounded, no meaning can be apprehended or ex-
pressed. But thought is also relation and connexion of
the things distinguished, and this aspect of it is equally
important with the other. Aristotle shows his one-sided-
ness — a one-sidedness which throws him into opposition
to Plato, but which enables him to correct Plato only by
falling into the opposite error — when he exclusively fixes
his attention on the " differentiating " aspect of knowledge,
and takes no notice of the " integrating " aspect of it. It
is easy to see that this exclusive attention to one side of
the truth may lead in many ways to a distorted view both
of the world and of the intelligence that apprehends it. If
Heraclitus be interpreted as simply denying the right of
thought to introduce its definiteness into the flux of sense,
nothing but absolute scepticism can come out of hii
philosophy ; and Aristotle was right in maintaining that it is
only as the flux is brought to a stand, and the universal is
fixed as a permanent and definite object of thought,' that
knowledge becomes possible. But, on the other hand, if
distinction be taken as absolute, if the definite assertion
of a thing be taken as a negation of all relation to what it ,
is not, if the fixity of thought be taken as an abstract self-
identity which excludes all the movement of finite things
wherein they show their finitude and pass beyond them-
selves into other things, then knowledge will be equally
impossible. Our consciousness, on such a theory, would
be disintegrated into parts which would o-rni no connexion
with each other ; nor would it be possible for us to think
of thing'! as, in spite of their difference.-, bound together into
the unity of one world. The law of contradiction or
distinction, therefore, is likely- to lead to serious miscon-
ceptions, unless it be complemented by a law of relation —
a law expressing the truth that there is a unity which
transcends all distinction. For all intelligible distinction
— all distinction of things in the intelligible world — must
be subordinate to their unity as belonging to that world,
and therefore essentially connected with each other and
with the intelligence. In such a world, in other words,
there can be no absolute distinctions or differences (not
even between being and not-being); for distinction without
relation is impossible, and a conception held in absolute
isolation from all correlated conceptions ceases to have
any meaning. This does not, of course, imply a neg-ation
of the law of contradiction within its own sphere, but it
does imply that that sphere is limited, and that there is no
absolute contradiction. All opposition is within a pre-
supposed unity, and therefore points to a higher reconcilia-
tion, a reconciliation which is reached when we show that
the opposition is one of correlative elements.
The great step in logical theory which was taken by the
idealistic philosophy of the post-Kantian period was simply
to dissipate the confusion which had prevailed so long
between that bare or formal identity, which is but the
beginning of thought and knowledge, and that concrete
unity of difference, which is its highest idea and end. It
was, in other words, to correct and complete the concep-
tions of thought as analytical, and as externally syntheti-
cal, by the conception of it as self-determining, to show
that it is a unity which manifests itself in difference and
opposition, yet in all this, even when it seems to be
dealing with an object which is altogether external to
it, is really developing and revealing itself. This new
movement of thought might, in one point of view, be
described as the addition of another logic to the logic
of analysis and the logic of inductive synthesis which
were already in existence. But it was really more than
this ; for the new logic was not merely an external addition
METAPHYSIC
97
to the old logics, it also put a new meaning into these |
logics by bringing to light the principles that were involved
in them. At the same time it broke down the division
that had been supposed to exist between logic and meta-
physic, between the form or method of thought and its
matter. It showed that thought itself contains a matter
from -which it canpot be separated, and that it is only by
reason of this matter that it is able to ask intelligent
questions of nature, and to get from nature intelligible
answers. A short space must be devoted to explain this
relation of the three logics to each other.
The anal)-tic logic fairly represents our first scientific
attitude to the world, in which we concentrate our attention
upon the facts as they are given in experience, with no
thought of any mental sjiithesis through which they are
given. To ourselves we seem to have to do with an object
which is altogether independent of our thought, and what
we need in order to know it is to keep ourselves iu a purely
receptive attitude. All we can do is to analyse what is
given, without adding anything of oui' own to it. It has,
however, already been pointed out that this apparent self-
abnegation is possible only because, in abnegating our indi-
•vidual point of view, we do not abnegate the point of view
that belongs to us as universal or thinking subjects. In
other words, the objectivity of knowledge thus attained is
not the ceasing of the activity of our tliought, but rather of
all that interferes with that activity. We seem to abstract
'from ourselves, but what we do abstract from is only the
individuality that stands between us and the world. The
scientific observer who has thus denied himself, however,
is not necessarily conscious of the meaning of what he has
done. • The immediate expression of his consciousnes.« is
not "I think the object," but "it, the object, is"; and the
more intensely active he is the more his activity is lost for
him in the object of it. His whole work is, for himself,
only the analysis of given facts, and for the rest he seems
to have nothing to do but to take the world as he finds
it. The voice of nature to which he listens is for him
aot Ills own voice but the voice of a stranger, and it does
not occur to him to reflect that nature could not speak to
any one but a conscious self. His business is to determine
things as they present themselves, to enumerate their
qualities, to measure their quantities ; and his logic accord-
ingly is a logic governed by the idea of the relative com-
prehension and extension of the things which he thus
names and classifies. Such an analytic logic seems to be
all that is necessary, because the only predicates by which
things are as yet determined are those which are involved
in their presence to us in perception, and as perceived, they
seem to be at once given in sjl their reality to the mind
that apprehends them. .
A step is taken beyond this first naive consciousness of
things, whenever a distinction is made between appearance
and reality, or whenever it is seen that the things perceived
ore essentially related to each other, and that therefore they
cannot be known by their immediate presence to sense, but
only by a mind which relates that which Ls, to that whii i
is not, immediately perceived. If " the shows of things are
least th ;mselves," we must go beyond the shows in order to
know them ; we must seek out the permanent for that
which is given as transient, the law for the phenomenon,
the cause for the effect. The process of thought in know-
ledge therefore is iio longer lost in its immediate object,
but is, partly at least, distinguished from it. For just in
proportion as the reality is separated from the appearance
doss the knower become conscious of an activity of his own
thought in determining things. From this point of view
nature is no longer an object which spontaneously reypals
itself to us, but rather one which hides its meaning from
03, and out of which we must WTing its secret by persistent
questioning. And, as this questioning process obviously
has not its direction determined purely by the object itself,
it becoiues manifest that the mind must bring with it Ihc
categories by which it seeks to make uatui-e intelligible.
To ask for the causes of things, or the laws of things, pre-
supposes that the immediate appearance of them does not
correspond to an idea of reality which the mind bring.s
with it, and by which it judges the appearance. Nature
is supposed to be given to or perceived by us as a multi-
tude of objects in space pasiing through successive changes
in time ; and what science seeks is to discover a necessity
of connexion running through all this apparently contingent
coexistence and succession and binding it into a system.
Science, therefore, seems to question nature by means of
an idea of the necessary interdependence and conue.xiou of
all thing.5, as parts of one systematic whole governed by
general laws — an idea which it does not get froni nature,
but which it brings to nature. Hence the logic in which
this process of investigation expresses its consciousness of
itself will be a synthetic logic, a logic built on certain prin-
ciples which are conceived to be independent of experience,
and by the aid of which we may so transform that experi-
ence, so penetrate into it or get beyond it, as to find for it
a better explanation than that which it immedL-.tely gives of
itself. The Posterior Analytic, in which Aristotle brings in
the idea of cause to vivify the syllogistic process, or supply a
real meaning to it, may already be regarded as a first essay
in this direction. And the theory of inductive logic, as
explained by Bacon and his successors down to Mill, is a
continuous attempt to determine what are the principles and
methods on which experience must be questioned, in order
to extract from it a knowledge which is not given in im-
mediate perception.
It was, however, Hume who first brought into a clear
light the subjectivity of the principles postulated in this
logic, and especially of the principle of causality, which is
the most important of them. In thus contrasting the sub-
jectivity of the principles of science with the objectivity
of the facts to which they are applied, it was his intention
to cast doubt on the science which is based on the applica-
tion of the former to the latter. The principles, he main-
tains, are not legitimately derived from the facts, therefore
they cannot legitimately be usad to interpret them. They
are due to the influence of habit, which by an illegitimate
process raises frequency of occurrence into the universality
and necessity of law, and so changes a mere subjective
association of ideas into an assured belief and exjjectation
of objective facts. The answer given by Kant to this
sceptical criticism of science involved a rejection of that
very opposition of subjective and objective upon "which it
was based. Without necessary and universal principles,
the experience of things as qualitatively and quantitatively
determined objects, coexisting in space and passing
through changes in time (or even the determination of the
successive states of the subject as successive), would itself
have been impossible. Hence necessity of thought cannot
be derived from a frequent e.xperience of such objects. It
is true tLat the determination of things as permanent sub-
stances reciprocally acting on each other, according to uni-
versal lawrs, goes beyond the determination of them as
qualified and quantified phenomena in space and time.
But both determinations are possible only through the
same a priori principle, and we cannot admit the former
determination without implicitly admitting the latter. As,
therefore, it is through the necessity and universality of
thought that objects exist for us, even before the application
to them of the principles of scientific induction, and as the
application of those principles is only a further step in
that a priori synthesis which is abready involved in the
perception of these objects, we have no reason for treating
198
.M E T A P H Y S I C
the former kind of synthesis as ohj actively valid which
does not equally apply to the latter.
This vindication of the principles of indiiction has, how-
ever, a further consequence, which was not clearly seen by
Kant. It is fatal to the antithesis of the " given " and
the '' known," of what is perceived and what is conceived,
of natura mo.terialiler spectata and nattera formalUer
apeclata, which he still admitted. For that antithesis
really rested on the idea that there is no universal and
necessary principle of determination of things involved in
the apprehension of them as qualified and quantified
phenomena in space and time. So soon, therefore, as it is
seen that there is such a principle, and that the fii-st deter-
mination if things as objects of perception is due to the
same a priori synthesis which determines them m the
second place as objects of experience, the ground for that
contrast between reality and appearance on which the
theory of induction rested is taken away. Kant, indeed,
finds a new meaning for that contrast by interpreting it as
referring, not to the opposition between things as they are
given and things as they are known, but to a supposed
opposition between things as they are given and known in
experience and things as they are in themselves out of
experience. This new antithesis of reality and appearance,
however, only means that the former antithesis has broken
down, and that therefore the ideal of knowledge based
upon it has yielded to a new ideal. The so-called things
in themselves are noumena, the objects of an intuitive or
perceptive understanding, i.e., objects in which the contrast
of perception and conception, of given and known, is tran-
scended. We can make Kant's theory consistent only by
supposing him to mean that the conception of the world as
a system of substances determining each other according
to universal laws does .not yet satisfy the idea of know-
ledge which reason brings with it. In other words, just
as science from the point of view of necessary law found
something wanting in the conception of the world as a
mere complex of quantified and qualified phenomena in
space and time, so philosophy, in view of a still higher ideal
of knowledge, may condemn the conception of the world
as a system of objects determined by necessary laws of
relation as itself inadequate and imperfect. And we have
seen that this higher ideal is that which is involved in
the unity of self-consciousness. Unfortunately Kant was
unable, as Aristotle had been unable, to distinguish this
idea from the idea of an abstract identity in. which there
is no room for even a relative difference of perception and
conception, and therefore the perceptive understanding was
named by him only to be rejected.
If, however, wo correct this inadequacy of Kant's state-
ment, as his later works enable us partly to correct it,
we see that it involves a new idea of knowledge and a new
logic, — a logic governed by the idea of organic unity and
development, just as the analytic logic h.ad been governed
by the idea of identity, and as the inductive bgic had been
governed by the idea of necessary law. For, if the unity
of self-consciousness be our type of knowledge, truth must
mean to us, not the apprehension of objects as seLf-identieal
tilings, distinguished from each other in quantity and
quality, nor even the determination of such things as
standing in necessary relations to each other. It must
mean the determination of the world (and of whatever in
it is in any sense an independent reality, so far as it is so
lindependent) as a unity which realizes itself in and through
difference, a unity which is indeed determined, but deter-
mined by itself. In a view of the world which is governed
by tliis category, correlation must be reinter{>reted as
organic unity, and causation as development. Its logical
method must be neither analytical nor sjmthetical, or
irather it must be both at once, i.e., it must endeavour to
exhibit the process of things as the evolution of a nnity
which is at once self-differentiating and self-integrating;
which manifests itself in difference, that through difference
it may return upon itself. Further, as this logic arises
simply out of a deeper consciousness of that which was
contained in the two previous logics, so it first enables us
to explain them. In other words, the ad\-ance from the
analytic to the inductive logic, and again from the inductive
to what may be called the genetic logic, may itself be
shown to be a self-determined development of thought, in
which the first two steps are the imperfect manifcs^tion
of a principle fully revealed only in the last step. The
consciousness of self-identical objects, independent of each
other and of thought, is thus only the beginning of a pro-'
cess of knowledge which reaches its second stage in the
determination of these objects as essentially related to each
other, and which finds its ultimate end in the knowledge
of the correlated objects as essentially related to the mind
that knows them. Or if, in this last point of view, things
are still conceived as having a certain relative independence
of the mind, it can only be in .so far as they are in the
Leibnitzian sense monads, or microcosms, — i.e., in so far as
they are self-determined, and so have, in the narrower circle
of their individual life, something analogous to the self-
completed nature of the world, when it is contemplated in
its unity with its spiritual principle.
Such a genetic logic is inconsistent with any absoluto
distinction between i\iQ a priori and a posteriori element
in knowledge. For here the a pjriori is not simply a law
of neces.?ary connexion to be applied to an external matter,
but a principle of organic development, a principle which,'
from the very nature of it, cannot be appUcd to a foreign
matter. To treat the world as organic is to apply to it a
category which is inconsistent with its being something
merely given or externally presented to thought. The^
relation of things to thought must it.?eLf be brought under,
the same category of organic unity which is apphed to the.'
relation of things to each other in the world, otherwise the'
externality of the world to the thought for which it is will
contradict the conception of the world as itself organic.
Hence the distinction of a jiriori and a posteriori, so far as'
it is maintained at all, must shrink to something secondary^
and relative. It can be .maintained only as a distinction
of thought from its object, which presupposes their ultimate
unity. From this point of view logic may be said to deal
with the a priori, in so far as it treats the general conditions
and methods of knowledge without reference to any parti-
cular object. Logic must e.xhibit abstractly the process by
which the intelligence establishes its unily with the intelli-
gible world; or, to jjut it in another way, it must demon-
strate tjjattlie being of 'things can be truly conceived only
as their being for thought. It is limited to the a priori, in
the sense that it ends with tlie idea that the esse of things
is their intdUgi, and does not consider how this real
intelligence or intelligible reality manifests itself in the
concrete world of nature and spirit.
In this sense logic cannot be .separated from metaphysic
if metaphysic be confined to ontology. They are simply
two aspects of one science, which we may regard either as
determining the idea of being or the idea of knowing.
The process of knowing is never really a forma! process; it'
always involves the application of certain ccfnjorif.'i, and'
these categories are simply successive definitions of being
or reality. We cannot separate the category from the
movement of thought by which it is evolved and applied,
nor the transition from lower to higher categories from
changes of logical method. Heace a logic divorced from
metaphysic inevitably becomes empty and unreal, and a
metaphysic divorced' from logic reduces itself to a kind of
dictionary of abstract terms, which are ^ut in no living
METAPHYSIC
90
relation to each other. For such a logic and such a meta-
physic must rest on the assumption of an absolute division
between being and thought, the very two terms the unity
of which it must be the utmost object of both logic and
metaphysic to prove and to produce.
4. The Rdalion of Mdaphysic to Philosophy of Eeli'jlon.
— The possibility of a "first philosophy," as we have
already seen, is essentially bound up with the possibility
of what we may call a last philosophy. It is only in so
far as we can rise above the point of view of the individual
bud the dualism of the ordinary consciousness — in so far,
in other words, as we can have at least an anticipative
consciousaess of that last unity in which all the differences
of things from each other and from the mind that knows
them are explained and transcended — that we are able to
go back to that first unity which all these differences pre-
suppose. The life of man begins with a divided conscious-
ness, with a consciousness of self which is opposed to the
consciousness of what is not-self, with a consciousness of a
multiplicity of particulars which do not seem to be bound
together by any one universal principle. Such division
and apparent independence of what are really parts of one
whole is characteristic of nature, and in spirit it is at first
only so far transcended that it has become conscious of
itself. A conscious difference, however, as it is a difference
in consciousness, is no longer an unmediated difference.
It is a difference through which the unity has begun to
show itself, and which therefore the unity is on the way to
subordinate. And all the development of consciousness
and self-consciousness is just the process through which
this subordination is carried out, up to the point at which
the difference is seen to be nothing but the manifestation
of the unity. Just so far, therefore, as this end is present
to us, — so far as we are able to look forward to the solution
or reconciliation of all the divisions and oppositions of
which we are conscious and to see that there is an all-
embracing unity which they cannot destroy, — is it possible
that we should look back to the beginning or first unity,
and recognize that these divisions and oppositions are but
the manifestations of it. Thus the extremes of abstractness
and of concreteness of thought are bound up together. The
freedom of intelligence by which we get rid of the complexity
of our actual life, and direct our thoughts to the simplest
and most elementary conditions of being and knowing, is
possible only to those who are not limited to that life, but
can regard it and all its finite concerns from the point of
view of the infinite and the universal. In this sense it is
true that religion and metaphysic spring from the same
source, and that it is possible to vindicate the rationality of
religion only on metaphysical principles. The philosophy
of religion is, in fact, only the last application or final
expression of metaphysic; and, conversely, a metaphysic
which is not capable of furnishing an explanation of religion
contradicts itself.
This last remark arfords us a kind of criterion of a true
metaphysic. Can it or can it not explain religion? If it
cannot, it must be eqxially unable to explain its own possi-
bility, and therefore implicitly it condemns itself. Thus a
pantheistic system, which loses the subject in the absolute
substance, cannot explain how that subject should appre-
hend the substance of which it is but a transitory mode, nor,
on the other hand, can it explain why the substance should
manifest itself in and to a subject. And the same criticism
maybe madeonalltheoriesin which thefirst or metaphysical
unity is abstractly opposed to the manifoldness and con-
tingency of things. Not only of Spinoza, but also of Kant,
of Fichte, and even of Schelling, it might with some truth
be said that their absolute is like the lion's den, towards
» which all the tracks are directed, while none come from it.
It. is essential that the first unity should be such as to
explain the possibility of difference and division, for, if it
is not, th^n the return to unity out of difference is made as
accidental as the difference itself. A^■hen Aristotle repre-,
sentcd the Divine Being as pure self-consciousness, pure!
form without matter, he found himself unable to account
for the existence of any world in which form was realized
in matter. AMien tierefore he speaks of the process of
the finite world by which it returns to God, and attributes
to nature a will, which is directed to the good as its final
cause, his theory seems to be little more than a metaphor
in which the analogy of consciousness is applied to the
unconscious. For, if the Divine Being is not ma"nifested
in the world, any tendency of the world to realize the good
becomes an inexplicable fact. A similar difficulty is, as
we saw, involved in Kant's confusion of the bare identity
of understanding with the absolute unity of knowledge.
Reducing the unity of self-consciousness to such a bare
identity, Kant could not be expected to see, what Aristotle
had not seen, that pure self-consciousness is essentially
related to anythiag but itself. Hence the various attempts
which he made in his ethical works and in his Criticism of
Judgment fo'fijida link of connexion between the noumenal
and the empirical were necessarily condemned even by him-l
self as the expressions of a merely regulative and subjective'
principle of knowledge. Even Fichte, who found in the!
thought, which is for him the prins of aU existence, a
principle of differentiation and integration which explained
how self -consciousness in us should be necessarily correlative'
with the consciousness of a world, was unable to free him-
self from the Kantian opposition of a noumenal identity
in which there is no difference to a phenomenal unity
which is realized in difference. Hence by him also the
return out of difference is regarded as an impossibOity, oi-
as a processus in infinitum, and the absolute unity as that
which is beyond all knowledge and otdy apprehended by
faith.
If we look to completely elaborated theories, and dis-
regard all tentative and imperfect sketches, it may fairly^
be said that all that has as yet been done in the region of
pure metaphysic is contained in two works, in the Meta-
physic of Aristotle and the Lo^ic of Hegel. And up to a
certain point the lesson which they teach is one and the
same, viz., that the 'oltimate unity which is presupposed
in all differences is the unity of thought with itself, the
unity of self-consciousness, and that in this unity is con-
tained the type of all science, and the form of all existence ;
in other words, I = I is the formula of the universe. The
difference between these two works has, however, already
been indicated. With Aristotle, because he neglects the
essential relation of self-consciousness to consciousness, vr
of the conscious self to the world of objects in space and
time, the unity of self-consciousness tends to pass, as it did
pass with the Neo-Platonists, into a pure identity without
diff'erence. In the Hegelian logic, on the other hand, self-
consciousness is interpreted as a unity which realizes itself
through difference and the reconciliation of difference — as,
in fact, an organic unity of elements, which exist only as
they pass into each other. In other words, it is shown
that the differentiating movement by which the subjective
and the objective self are opposed and the integrating
movement by which they are retinited are both essentiaLj
Hence we cannot think of the conscious self as a simple^
resting identify, but only as an active self-determining
principle ; nor can we think of its self-determination as a
pure affirmation of itself, without any negation, but only
as an affirmation which involves a double negation — <in
opposition of two elements which yet are essentially united.
Each factor in this unity, in fact, is necessarily conceiv.il
as passing beyond itself into the other; the subject i
subject OAly as it relates itself to the object, the objegLia
loa
:aXETAPHYSIC
object only as it relates itaelf to the subject. It is this
tension against each other of elements which yet are corre-
kted and indissolubly united, this self-surrender to each
other of elements which yet are maintained in their distinc-
tion, which constitutes the organic unity of thought in
itself, and separates it from the mere abstract unity of
mysticism. A\Tien, however, the concrete or self-differen-
tiating character of the unity of self-consciousness is appre-
hended in this way, — so that it is imijossible to confuse its
indivisible unity with the simplicity of that which is one
rrierely because it has no differences in it, — the problem of
the relation of pure self-consciousness to the world in space
and time ceases to be insoluble. Thought, as it is seen io
have difference in itself, is no longer irreconcilable with
t!\e world of difference ; nor is it necessary to introduce a
foreign v\rj to make their connexion intelligible. For, as
thought is a principle of difference as well as of unity, of
analysis as well as of synthesis, and as it cannot realize
itself in its unity except through the utm.ost development
of difference, abstract self-consciousness, with its transparent
or merely ideal difference, cannot be its ultimate form.
On the contrary, the consciousness of self is possible oii'y
in distinction from, and in relation to, a world of objects.
In other words, the unity of the thinking subject pre-
supposes, not merely the opposition of the subjective and
the objective self, but also the opposition of the self in its
pure self-identity to a world of externality and difference.
The pure intelligence, which is the pruis of all things, must
not, therefore, be regarded — as Aristotle regarded it — as
merely theoretical, but also as practical. It must be con-
ceived as a living principle, a principle which only in self-
manifestation can be conscious of itself, and to the very
nature of which, therefore, self-manifestation is .essential.
In this way Hegel — just because ho grasped the concrete
character of the unity of thought in itself — was enabled to
understand the necessary unity of thought or self-conscious-
ness with the world, and to heal the division of physics
from metaphysic, which Aristotle had admitted.
Sohelling and others who have raised objections to the
Hegelian method have specially directed their criticisms
against this transition from logic to the philosophy of
nature, from pure self-consciousness to the external world
in space and time. In doing so, they have practically
fallen back upon the Aristotelian theory, with its opposition
of God, as pure form, to the finite world. But this in effect
is to deny that " the real is the rational " or intelligible,
and to introduce into the world, as the ground of its
distinction from reason, a purely irrational or contingent
element. A modern follower of Schelling's later positive
])liilosophy only draws the necessary consequence from this
view when he teaches the pessimist creed that the highest
good is the negation or extinction of the finite. Nor can
we wonder that the same writer who denies that the
absolute self-consciousness is essentially related to or
manifested in the world should proceed to reduce this
self-consciousness to a mystic identity which comes out of
itself and becomes self-conscious only by an inscrutable
act of will. The fact, indeed, that those who deny the
possibility of a rational transition from self- consciousness
to the world are forced by the logic of their position to
reduce self-consciousness to an abstract identity may be
regarded as a kind of indirect proof that the principle of
self-consciousness, truly conceived, does involve that transi-
tion. Another step in the same direction may be made if
we consider how the Cartesian philosophy treated the same
opposition, which it also regarded as absolute. By
Uescartes mind and matter, thought and extension, are
defined as abstract oppositos, every quality of each finding
its contradictory counterpart in a quality of the other.
Miad is a pure self-determined unity, which is as it knows
itself and knows itself as it is, which has no discretionoi
parts or capacity of division or determination from « ithoui
Matter is essentially discrete or infinitely divided ; it is »
pure passivity ; and all its determination comes to it from
without. The world is therefore, as it were, "cut in tw«
with a hatchet," divided into two unrelated existences,
which are held together only by the will of God. Spinoza
cuts the knot, and avoids the arbitrariness of this solution,
by treating' extension and thought as two attributes
separated only in respect of our intelligence, but each
expressing fully the absolute substance. And something
like the same view has been revived in recent times, by
writers like Lewes and ilr Spencer, who speak of feelings
and motions as two opposite " aspects " of the same fact.
AVhen we ask, however, for whom these attributes or
aspects are a unity, it becomes clear that the intelligencB
which is regarded as standing on one side of the dualism
must also be taken as transcending it, and relating the two
sides to each other. Moreover, the correspondence of ths
two attributes upon which Spinoza insists and their contra-
riety upon which Descartes insists, when taken together,
give us the idea of a correlative opposition, i.e., of an opposi-
tion of elements which yet are necessary to each other.
If, therefore, they cannot be simply identified as Spinoza
identifies them, yet they need no external bond such as
Descartes introduces to combine them ; for they cannot
exist apart from each other. Their opposition is held
within the limits of their unity, and is no absolute con-
tradiction, but rather an opposition which exists only as it
is transcended. In other words, it is an abstract opposi-
tion, i.e., it is an opposition of elements which seem to be
irreconcilable till it is observed that they are correlative,
that each exists or has a meaning only as it relates itself
to, or passes out of itself into, the other, and that each,
held in its abstraction and separation from the other, loses
all the meaning that it seemed to have. For, as in an
orj-.mic body each member or orga.n lives only in tension
against the othens, yet only as continually relating itself to
the others, so the utmost opposition of mind to matter, of
the intelligence to the intelligible world, presupposes their
unity, and is only the realization of i
There is here, however, something more than an ordinary
case of correlation, for in this unity of opposites mind
appears t^vice, once as one of the opposites, and again
as the unity which transcends the opposition. This
ambiguity becomes most obvious in theories like that of Mr
Spencer, who speaks of " two consciousnesses," which cannot
be resolved into each other, but yet which strangely form
inseparable parts of one and the same consciousness. What,
however, is really involved in such a statement is that the
external world, which in the £rat instance presents itself
as absolutely opposed in nature to the subject whose object
it is, is yet one with that subject, and that therefore tho
antagonism of mind to its object is only the last differentia-
tion through which it realizes its unity with itself. In
Hegel's language, that which presents itself as other than
mind is ils other — "an other which is not another," whose
difference and opposition to itself it overreaches and over-
comes. We must, therefore, regard the independence and
externality of nature, its indifference, and even, as it seems,
opposition, to tho development of the moral and intellectual
life of man, as merely apparent. For man, in this point
of view, is not merely one natural being among others, but
the being in whom nature is at once completed and
transcended. If, therefore, at first he appears to stand
in merely accidental and external relations to the other
existences among which he finds himself, yet tho whole
process of his life — tho process liy which ho comes to know
the external world, and by wliich, reacting upon it, ho
make.s it the mr^ans to the reali/.ution of an individual and-
METAPHYSIC
101
•ocieJ life of hia own — is the negation of tliis contingency
and externality. In all this process he is showing himself
to be a being who can only know himself as he knows the
objective world, and who can only realize himself as he
makes himself the agent of a Divine purpose, to which all
things are contributing.
Such an idea of man's relation to the world is necessarily
involved in any theory that goes beyond that subjective
idealism or sensationalism which denies to him every
©bject of knowledge except his own states of feeling, and
every end of action except his own pleasures and pains,
flecent speculation, indeed, has suggested a compromise by
which this dilemma is supposed to be evaded, and mankind
are represented as forming an organic unity in themselves,
though they are still conceived as standing in an external
and accidental relation to nature, the forces of which by
tu6ir knowledge and skill they have subdued and are more
and more subduing to their service. Such a compromise
We find in the philosophy of Comte, the first writer who,
starting from an apparently empirical basis, was able to
break through the individualistic prejudices of the school of
Locke. In the latter volumes of his Positive Philosophy,
still more in his Positive Politics, Comte so far transcends
individualism as to deny the externality of men to each
•ther, aud to declare that " the individual, as such, is an
abstraction," and that in reality he cannot be separated
from the social organism, which is thus not merely an
extraneous condition of his development, but essential to
his very existence as man. Thus individual men exist
only through the viniversal — through the spirit of the
family, of the nation, of humanity, which manifests itself
in them as a principle of life and development. Yet this
organic unity, according to Comte, is in contact with a
world which in relation to it is external and contingent.
Nature has not its final cause in man, but on the contrary is,
at first, rather his enemy ; and it is to humanity itself that
the praise is due if to a certain extent the enemy has been
turned into a servant. The unity of life which manifests
itself in humanity cannot therefore be considered as a
■niversal principle, as the princii^le of the whole universe,
but simply as the principle of the limited existence of man,
which is hemmed in on evei-y side by external and, in the
iriaiu, ur inown conditions. If humanity therefore is an
Organism, it is an organism existing in a medium which in
reference to it is inorganic, i.e., in a medium which has no
essential relation to the life which animates man.
It is obvious, however, that this theory is an illogical
attempt to find a standing ground between two opposite
philosophies, — between the philosophy which treats man
merely as a natural individual, placed among other individual
beings and things, and which therefore regards his relation
to them as something accidental and external, and the philo-
sophy which treats him as a spiritual subject, a conscious
and self-conscious being, and regards him therefore as having
■o merely external relations either to other men or to nature.
Comte shrinks from regarding the world without us as the
manifestation of that spiritual principle which is also within
«s, which constitutes our very nature as individual men,
and therefore connects us with the world at the same time
tiiat it separates us from it. Yet he recognizes the
existence in lis of a principle which is so far universal that
ft constitutes a community between all men. He thinks
that the individual can transcend himself, so far as to see
all things, not indeed from a Divine point of view, siih
^ecie sctemitatis, but from the point of view of universal
humanity, and that in conformity with this theoretical
oonsciousness, he can live a practical life of altruism, i.e.,
f a life in which ho identifies his own good with the good of
humanity. But the philosophy that has gone so far must
logically go further. It is impossible to treat humanity as
an organism without extending the organic idea to the con-
ditions under which the social life of humanity is develoi>ed.
The medium by aid of which, or in reacting against
which, the organized being maintains itself is an essentui
part of its life ; it remains organic only in so far as it can
mould itself to its conditions, and its conditions to itself.
This is true even of the animal organism in relation to its
small circle of conditions, which, however, is part of a
larger circle to which the animal has no relation. But a
conscious being is a universal centre of relations ; there is
nothing which it, as conscious, cannot make part of its own
life. Hence the application of the organic idea to it in-
volves its application to the whole world. And, if the
recognition of a universal principle manifested in humanity
naturally led Comte to the idea of the worship of humanity,
the recognition of a universal principle manifested in man
and nature alike must lead to the idea of the worship of
God.
The rationality of religion, then, rests on the possibility
of an ultimate synthesis in which man and nature are
regarded as the manifestation of one spiritual principle.
For religion involves a faith that, in our efforts to realize
the good of humanity, we are not merely straining after
an ideal beyond us, v/hich may or may not be realized, but
are animated by a principle which within us and without
us is necessarily realizing itself, because it is the ultimate
principle by which all things are, and are known. This
absolute certitude that we work effectually becau.se all the
universe is working with us, or, in other words, because
God is working in us, can find its explanation and defence
only in a philosophy for which " the real is the rational,
and the rational is the real." And such a philosophy,
beginning with the Kantian doctrine that existence means
existence for a spiritual or thinking subject, must go on
to prove that that only can exist for such a subject which
is the manifestation of thought or spirit ; and, conversely,
that spirit or intelligence is essentially self-manifesting, or,"
in other words, that it carmot be conceived except as
standing in essential relation to an external and material
world. Finally, if nature be thus regarded as a necessary;
manifestation of spirit, it can be opposed to spirit only in'
so far as spirit in its realization becomes opposed to itself.'
In other words, nature must be regarded as, from a higher
point of view, included in .spirit. Nature exists that it
may show itself to be spiritual in and to man, who
transcends it yet implies it, who finds in it the necessary
basis of his thought and action, but only that he may build
upon it a higher spiritual life.
K.iture is made better by no mean
But nature makes that mean : so over the art
Which, you say, adiJs to nature is au art
Which nature makes. "
Only the order of precedence suggested by these words
must be inverted. For, as nature only is for spirit, so,
the spiritual energy which reacts upon nature is that
which manifests for the first time what nature in reality
is. It is the consciousness of this — i.e., t>i the identity of
that which is realizing itself within and without us, — the
consciousness that the necessity which is the precondition
of our freedom is the manifestation of the same Epirit
which makes us free — which turns morality into religion.
For it is this alone which enables us to regani the realization
of the highest ends of human life as no mere happy accident,
or as a conquest to be won by the cunning of man from an
unfriendly or indifferent destiny, but as the result towards
which all things are working.
In this philosophy, which finds its most adequate
e.xpression in the works of Hegel, there are two things
which may be distinguished — the general idealistic view of i
the world, and the dialectical movement of thought ha!
102
METAPHYSTC
which Hegel dovelofs and expresses it. And there are
perhaps many at the present time who are prepared to
accept the former, but who yet suspect, or eveu reject, the
latter. And no doubt there is much in Hegel's Logic and
Philosophy of Spirit, and still more in his Philosophy of
Xriture, which there is reason to regard with distrust.
Til clever hands that are not checked by a sufficient con-
Roiousness of the whole, the Hegelian dialectic may be
Tiii^de into the means of producing a seeming proof of any-
•thing. Nor is it always easy to determine how far Hegel
himself was tempted by an impatient consciousness of the
universality of his method to employ it in case- where the
conditions of its successful application were wanting.
Sometimes he seems to forget, what he himself teaches, that
science must first have generalized e.xpsrience and deter-
mined it by its finite categories, ere it is possible for
philosophy to give its final interpretation. Yet, when we
realize the nature of that interpretation, and of the trans-
formation of science which philosophy by means of it
proposes to effect, it becomes clear that the dialectic of
Hegel is no extraneous addition to his idealism, but is part
and parcel of the same movement of thought. For this
dialectic rests on the idea that thought or self-conscious-
ness finds in its own organic unity the ultimate key to all
difficulties in regard to the objects of thought and their
relations to each other and to the mind. Self-consciousness,
as- has been already shown, is implicitly the whole web
of categories which it throws over the world, and by aid
of which it makes the world intelligible. All these it
contains in itself; and, as it proceeds to determine the
meaning of things, it simply produces its store, and
exhausts itself on the object. Now, if it be idealism, in the
strict sense of the word, to make thought or self-r.onscious-
ness the principle and ultimate explanation of all that
exists, it is obvious that we cannot separate idealism from
Buch a dialectic as this, which is nothing more than the
mind's consciousness of its o\vn movement or process of
Belf-a£Brmation. If to find thought in things be more than
an empty word, then the movement or process which
thought is must explain at once the transition from
thought to what in opposition to it we call " things," and
must give us the means of reconciling that opposition. In
other words, the same movement by v/hich thought deter-
mines itself as self-conscious, i.e., as a unity realized through
difference, must also be conceived as the explanation of the
difference between pure thought and the world, and as the
solution of that difference in the idea of absolute spirit.
Such idealism has a close relation to Christianity ; it may
be even said to be but Christianity theorized. It has often
been asserted that Hegel's philosophy of religion is but an
artificial accommodation to Christian doctrine of a philo-
sophy which has no inherent, relation to Christianity. If,
however, we regard the actual development of that philo-
sophy it would be truer to say that it was the study of
Christian ideas which first produced it. Wliat delivered
Hegel from the mysticism in which the later philosophies
of Fichte and Schelling tended to lose themselves, and led
him, in his own language, to regard the absolute " not
merely as substance but as. subject," — what made him
recognize with Fichte that the absolute principle is spiritual,
and yet enabled kim with Schelling to see in nature, as
the opposite of spirit, the very means of its realization, —
was his thorough appreciation of the ethical and religious
meaning of Christianity. In the great Christian aphorism
that " he who loseth his life alone can save it " he found
a, key to the difficulties of ethics, a reconciliation of
hedonism and asceticism. For what this saying implies
is that a spiritual or self-conscious being is one who is in
c.^ntradiction with himself when ho makes his individual
ei'!f his end. In opposing his own interest to that of
others, he is preventing their interests from becoming hlaj
all things are his, and his only, who has died to himselt
But if this be the truth of morality, it is something more,
for " morality is the nature of things." Wo cannot separate
the law of the life of man from the law of the world ia
which he lives. And, if it is the nature of things, as it ii<
the nature of spirit, that he who loseth his life shall save
it, the world must be referred to a spiritual principle, and
the Christian doctrine of the nature of God is only tha
converse of the Cliristian law of ethics. To Hegel, starting
from this point, a new light was thrown on (he Fichtean
treatment of the idea of self, and the Fichtean proof that the
consciousness of self implies a relation to an object which
is opposed to the self, and which yet from another poiol
of view — since an objoct exists only for a subject — cannot
be anything but an element of its own life. It was seen
that this movement of thought is no mere fluctuation
between contradictory positions, to be terminated finally by
an ipse dixit of faith, but that the unity of the opposite
elements is apprehensible by the intelligence, and ' that
indeed it ia its presence to the intelligence which makes
the consciousness of opposition possible. It was in this
sense that Hegel could say that that unity of opposites
which had been called unintelligible by previous writers
was just the very nature of the intelligence, and that only
a view of the world guided by this idea could be properly
intelligible, while every other view must contain in il
an unsolved contradiction, an element that remains per-
manently impervious to thought.
The great objection to a metaphyslc like this, at least
an objection which weighs much in the minds of many,
is that which springs from the contrast between the claim
of absolute knowledge which it see:ns to involve and the
actual limitations which our inteUigence encounters in
every direction. If the theory were true, it is felt we
ought to be nearer the solution of the problems of oni
life, practical and speculative, than we are ; the riddle of
the painful earth ought to vex us less; we ought to
find our way more easily through the entanglement of
facts, and to be able to deal with practical difficulties in a
less tentative manner. Yet there is really no antagonism
between such a doctrine and a consciousness of the limitar
tion of our faculties ; nay rather, it is only on such a
theory that a rational distrust of ourselves can be based.
When Aristotle meets the warning that we should think
finite and human things since we are finite and human
with tlie answer that we ought rather, so far as in us lies,
to rise to what is immortal and divine, he is not denying
the limits of man's knowledge and power ; on the contrary,
he is rather pointing to the very principle which makes us
conscious of those limits ; for it is just because there is io
man a principle of infinity that he knows his finitude, and,
conversely, it is just in the consciousness of this finitude that
he rises above it. A rational humility is possible only to
one who has in himself the measure of his own weakness,
and who, if he " trembles like a guilty thing surjirised," is
yet conscious that he is trembling before himself. This
truth is often expressed by Kant with special relation to
the moral consciousness, as where he contrasts the limitation
of man, as a sensible being, occupying an infinitesimal space
in the boundless world of sense, with his freedom from all
limitation as a personal self, a member of the truly infinite
world of intelligence. But it is not necessary to adopt
Kant's abstract division of the sensible from the intelligible
world to see that the consciousness of the greatness of the
problem which has to be solved in human life and thought
is deepened and widened by that very idea of philosophy
which yet gives us the assurance that the problem is
not insoluble, and even that, in principle, it is already
solved (.^- 9:)
ME T — ]\I E T
10^
METAPONTUM, or ilETAPO^TTOii (the first form is that
■generally found in Latin writers, but Thucydides, Strabo,
And other Greek authors employ the latter form), was a
city of Mcgiia Grjecia situated on the Gulf of Tarentum,
near the mouth of the river Bradanus, and distant about
24 miles from Tarentum and 11 from Heraclea. It was
founded by an Achaean colony about 700 b.c., though
various traditions existed which assigned it an earlier
origin. But according to the only historical account it
was a joint foundation from Sybaris and Crotona, to
which, as usual in similar cases, was joined a body of fresh
settlers from the mother country, under the command of a
leader named Leucippus. The object of its establishment
was without doubt to strengthen the Achaean element in
Magna Grsecia, as opposed to the increasing power of the
Tarentines, but at the same time to occupy a territory
which was remarkable for its fertility. It was to this
cause that lletapontum owed the great prosperity to which
it attained at an early period, and appears to have continued
to enjoy for several centuries, though it never assumed a
prominent place in history. It was, however, one of the
cities that played a conspicuous part in the political troubles
arising from the introduction of the Pythagorean principles
into the cities of lilagna Grscia, and it was there that the
philosopher himself ended his days. His tomb was still
shown there in the time of Cicero.
At the time of the Athenian expedition to Sicily
(415 B.C.) Metapontmn appears to have been an opulent
and powerful city, whose alliance was courted by the
Athenians ; but they contented themselves with a very
trifling support. In 332 b.c, at the time of the expedition
of Alexander, king of Epirus, into Italy, it was one of the
first cities to espouse his cause, and enter into an alliance
with him ; and they appear to have in like manner lent an
active support to Pyrrhus at a later period. Down to this
time, therefore, Metapontura seems to have retained its
position as one of the principal cities of JFagna Gra'cia,
and there is no evidence of its having suffered materially
from the establishment of the Lucanians in its immediate
neighbourhood. Nor have we any account of the precise
period at which it passed under the dominion of Rome, or
the conditions under which it became subject to the great
republic. But it was the Second Punic War which gave
the fatal blow to its prosperity. After the battle of C-iun»
in 216 B.C. it was among the first cities in the south of
Italy to declare in favour of Hannibal, and after the fall of
Tarentum in 212 B.C. it not only received a Carthaginian
garrison, but became for some years the headquarters of
Haimiba!. Hence, when the defeat of Hasdrubal at the
Metaurus (207 B.C.) compelled him to abandon this part
of Italy, and withdraw into the fastnesses of Bruttium, the
whole mass of the inhabitants of Jfctapontum abandoned
their city, and followed him in his retreat.
From tills time Metapontum sunk into a poor and incon-
iiiderable town ; though it was still existing as such in
the days of Cicero, it soon fell into complete decay, and
Pausanias tells us that in his time nothing remained of it
but a theatre and the circuit of the walls. All remains of
these have since disappeared, but the site is still marked
by the ruins of a temple, which occupy a slight elevation
on the right bank of the river Bradanus, about 2 miles
from its mouth. The sun-ounding plain, so celebrated in
ancient times for its fertility, is now desolated by malaria,
and almost uninhabited ; and the remains of the city itself,
between the site of the temple and the sea, are in great part
burled in the alluvial deposits of the neighbouring rivers.
Some excavations were carried on upon the spot by the
JJuc de Luynes in 1S28, and the results of his researches
Vero published by him in a special work (Mclaponlc, fol ,
t>8jis. 1833>.
JIETASTASIO (1695-1782). Pictro Trapassi, tho
Italian poet who is better known by his assumed name of
Metastasio, was bom in Piome, January 6, 109S. His
father, Felice Trapassi, a native of Assisi, came to Rome
and took service in what was termed the Corsican rcgin\ent
of the papal forces. He subsequently married a Bologiiesc
woman, called Francesca Galasti, and established himself
in business as a sort of grocer in the Via dei Cappellari.
Two sons and two daughters were the fruit of this niaiTiage.
The eldest son, Leopoldo, must bo mentioned, since he
played a part of some importance in the poet's life.
Pietro, while quite a child, showed an extraordinary talent
for improvisation, and often held a crowd attentive in the
streets while he recited impromptu verses on a given subject.
It so happened that, while he was thus engaged one evening
in the yeai 1709, two men of high distinction in Eonian
society passed by and stopped to listen to his declamation.
These were Gian Vincenzo Gravina, famous for legal and
literary erudition, famous no less for. his dictatorship of the
Arcadian Academy, and Lorenzini, a critic of some uoto.
Gravina was at once attracted by the boy's poetical talent
and by his charm of person ; for little Pietro was gifted
with agreeable manners and considerable beauty. The
great man interested himself in the genius he had accident-
ally discovered, made Pietro his proteg^, and in the course
of a few weeks adopted him. Felice Trapassi was glad
enough to give his son the chance of a good education and
introduction into the world under auspices so favourable.
Gravina, following a fashion for which we may find pre-
cedents so illustrious as that of Melanchthon, ReUenized
the boy's name Trapassi into Metastasio ; and this name
remained with him for life. Gravina intended his adopted
son to be a jurist like himself. He therefore made the boy
learn Latin and begin the study of law. At the same time
he cultivated his literary gifts, and displayed the youthful
prodigy both at his own house and in the Roman coteries.
Jletastasio soon found himself competing with the most
celebrated improvisatori of his time in Italy. Days spent
in severe studies, evenings devoted to the task of improvis-
ing eighty stanzas at a single session, were fast ruining
Pietro's healih and overstraining his poetic faculty. At
this juncture Gravina had to journey into Calabria on
business. He took Jletastasio with him, exhibited him in
the literary circles of Naples, and then placed him under
the care of his kinsman Gregorio Caroprese at a little place
called ScaMa. In counti-y air and the quiet of the southern
sea-shore Jletastasio's health revived. It was decreed by
thn excellent Gravina that he should never improvise a
line again. His great facility should be reserved for
nobler efforts, when, having completed his' education, he
might enter into competition with poets who had be-
queathed masterpieces to the world.
Metastasio responded with the docility of a pliant nature
to his patron's wishes. At the age of twelve, while attend-
ing to classical and legal studies, he translated the Iliad into
octave stanzas; and two years later he composed a tragedy in
the manner of Seneca upon a subject chosen from Trissino's
Italia Liberata — Gravina's favourite epic. It was called
Gi'uftino. Gravina had it printed in 1713 ; but the play is
lifeless; and forty-two years afterwards we find Jletastasio
WTiting to his publisher, CaLsabigi, that he would willingly
suppress it. Caroprese died in 1714, leaving Gravina his
heir ; and in 1718 Gravina also died. Metastasio inherited
from the good old man a property, consisting of house, plat?,
furniture, and money, which amounted to 15,000 scudi, or
about £4000. At a meeting of the Arcadian Academy,
amid the tears and plaudits of that learned audience, he
recited an elegy on the patron who had been to him so true
a foster-father, and then settled down, not it seems without
real sorrow for his loss, to enjoy what was no inconsiderable
104'
METASTASIO
fortune at that period. Jletastasio was now twenty.
During the la»t four years he had worn the costunae of
abbe, having taken the minor orders without which it was
then useles:i to expect advancement in Rome. His romantic
history, personal beauty, charming manner.?, and distin-
guished talents made him fasliionablo. That before two
years were out he had spent his money and increased his
reputation for wit will surprise no one. He now very
sensibly determined to quit a mode of life for which he
was not born, and to apply himself seriously to the work
of his profession. Accordingly ho went to Naples, and
entered the office of an eminent lawyer named Castagnola.
It would appear that be articled himself as clerk, for
Castagnola, who was a stern master, averse to literary
trifling, exercised severe control over his time and energies.
While .slaving at the law, Metastasio did not wholly neglect
the iluses. In 1721 he composed an epithalamium, and
probaWy also his first musical serenade, Endimione, on the
occasion of the marriage of his patroness the Princess
Pinelli di Sangro to the Marchese Belmonte Pignatelli.
But the event which fi.\ed his destiny was the following.
In 1722 the birthday of the empress had to be celebrated
with more than ordinary honours, and the viceroy applied
to Metastasio to compose a serenata for the occasion. He
accepted this invitation with mingled delight and trepida-
tion ; for Castagnola looked with no favour on his clerk's
poetical distractions. It was arranged that his authorship
should be kept a profound secret. Under these conditions
Metastasio produced Gli Orti Espcridi. Set to music by
Porpora, it won the most extraordinary ap])lause. The
great Roman prima donna, Marianna Bulgarelli, called La
Romanina from her birthplace, who had jjlayed the part
of Venus in this drama, was .so enraptured with the beauties
of the libretto that she spared no pains until she had dis-
covered its author. Asked point-blank whether he had
not written the words of the successful play, Metastasio
was obliged to answer, Yes ! La Romanina forthwith took
possession of him, induced him to quit his la\vyer's office,
and promised to secure for him fame and independence, if
he would devote his talents to the musical drama. It was
thus that the opera, already partially developed by the
Caesarean poet, Apostolo . Zeno, attained perfection. The
right man had been found for maturing this form of art
which the genius of the age demanded, but which was still
but incomplete. In La Romanina's house Metastasio
became acquainted with thegreatest composers of the day, —
with Porpora, from whom he took lessons in music ; with
Hasse, Pergolese, Scarlatti, Vinci, Leo, Durante, Marcello,
all of whom were destined in the future to set his plays to
melody. Here too he studieil the art of singing, and
learned to appreciate the stylo of such men as Farinelli.
His singularly pliant genius discerned the conditions which
the drama must obey in order to adapt itself to music in
the stage it then had reached. Gifted himself with extra-
ordinary facility in composition, and with a true poetic
feeling, he found no ditliculty in producing plays which,
while beautiful in themselves, judged merely as works of
literary art, became masterpieces as soon as their words
were set to music, and rendered by the singers of the
greatest school of vocal art the world has ever seen. Read-
ing Metastasio in the study, it is impossible to do him
justice. Our only chance of rendering him a portion of
his due is to approach these lyrical scenes — so passionate
in their emotion, so cunningly devised for musical effect —
with the phrases of Pergolese or Paesiello ringing in our
ears, and to imagine how a Farinelli or a Caffariello voiced
those stanzas which demand for their artistic realization
the " link6d sweetness long drawn out " of melodies as the
Italian school developed them. In short, Metastasio is a
poet nrjose poetry leapt to its real life in the environment
of music. The conventionality of all his plots, tha'
absurdities of many of his situations, the violence he does
to history in the persons of some leading characters, his
" damnable iteration " of the theme of love in all its
phases, are explained and justified by music. He can stilt'
be studied with pleasure and jjrofit. But our only chancei
of understanding the cosmopolitan popularity he enjoyedi
is by remembering that at least one half of the effect he
aimed at has been irrecoverably lost.
Metastasio resided with La Romanina and her husband
m Rome. The generous woman,- moved by an affection half |
maternal half romantic, and by a true artist's admiration
for so rare a talent, adopted him more passionately even'
than Gravina had done. She took the whole Trapassi
family — father, mother, brother, sisters — intoher ovra hotise.
She fostered the poet's genius and pampered his caprices.
Under her influence ho wrote in rapid succession tho
Dkhne Ahhandonata, Catonf in Utica, Em, Alessandr*
neW Indie, Scmiramide Riconosciuta, Siroe, and A rlaserse. '
These dramas were set to music by the chief composers of
the day, and performed in the chief towns of Italy. Every
month added to Metastasio's rerio\\Ti. But mc.inwhile La
Romanina was growing older; she had ceased to sing iu
public ; and the poet felt himself more and more dependent
in an irksome sense upon her kindness. He gained 300
scudi (about X60) for each opera ; this pay, though good,
was precarious, and he longed for some fixed engagement.
Abandoning himself gradually to despondent whims and
fancies, it became clear that some change in his condition
was desirable. And the opportunity for a great change
soon presented itself. In September 1729 he received
the offer of the post of court poet to the theatre at Vienna,
with a stipend of 3000 florin.?. This he at once accepted.
La Romanina unselfishly sped him on his way to glory. '
She took the charge of his family in Rome, and he set off
for Austria.
In the early summer of 1730 Metastasio settled at
Vienna in the house of a Spanish Neapolitan, Niccoli
JIartinez, where he resided until his death. This date
marks a new period in his artistic activity. Between the
years 1730 and 1740 his finest dramas, Adriano, Danetrio,
Issipile, Demofoontc, OHmpiade, C'lcmen:a di Tito, AchilU
in Sciro, Tcmistocle, and Altilio liiyolo, were produced for
the imperial theatre. Some of them had to be composed'
for special occasions, with almost incredible rapidity — the
Achille in eighteen days, the Ipermnesira in nine. Poet,'
composer, musical copyist, and singer did their work
together in frantic haste. The impress of the peculiar
circurhstances under which they were created is still left
upon them, not only in negligence of style, but also in an
undefinable quality which marks them out as products of
collaboration. But what must always surprise us is that
they should be as good as they are. Jletastasio understood
the technique of his peculiar art in its minutest details.
The experience gained at Naples and Rome, quickened by
the excitement of his now career at Vienna, enabled liira,
almost instinctively, and as it were by inspiration, to hit the
e.xact mark aimed at in the opera.
At Vienna Metastasio met with no marked social
success. His plebeian birth excluded him from aristocratic
circles. But, to make up in some nic-xsure for this com-
jiarative failure, he enjoycil the intimacy of a great lady,';
the Countess Althann, sister-in-law of his old patroness the
Princess Belmonte Pignatelli. She had lost her husband,
and had some while occupied the post of chief favourite ta
tho emperor. Metastasio's liaison with her became so close
that it was even believed they had been privately married.
From his letters to his friend La Romanina, and to the,
great singer Farinelli, who reigned supreme at the courti
of Madrid, we learn the littli details of the poet's life inj
M 'E ,T — M E T
105
its weftrisoms's monotony," and' come^ to comprehend his
.haracter, at once generous and timid, selfish and amiable,
prudent almost to excess of caution, and personally cold in
contradiction with the fervour of his sentimental muse.
The even tenor of this dull existence was broken in the
year 1734 by the one dark and tragic incident of his
biography. It appears that La Romanina had at last got
tired of his absence. Little satisfied with his friendly but
somewhat reticent communications, impitient to see him
once again, inquisitive perhaps about the terms on which
he lived vdth his new mistress, she resolved to journey to
^enna. Could not Metastasio get her an engagement at
the court theatre 1 The poet at this juncture revealed his
own essential feebleness of chafacter. To La Romanina he
owed almost everything as a man and as an artist. But
he was ashamed of her and tired of her. He vowed she
should not come to Vienna, and wrote dissuading her from
the projected visit. The tone of his letters alarmed and
irritated her. It is probable that she set out from Rome,
but died suddenly upon the road. Nothing can be said for
certain about her end, or about the part which Metastasio
may have played in hastening the catastrophe. All vre
know is that she left him her fortune after her husband's
life interest in it had expired, and that Metastasio, over-
whelmed with grief and remorse, immediately renounced
,the legacy. This disinterested act plunged the Bulgarelli-
;Metastasio household at Rome into confusion. La
Romanina's widower married again. Leopoldo Trapassi,
and his father and sister, were thrown upon their own
resources. The poet in Vienna had to bear their angry
expostulations upon his ill-timed generosity, and to augment
ithe allowances he made them.
As time advanced the life which Metastasio led at
iVienna, together with the climate, told upon his health
and siiirits. From about the year 1745 onward he writes
complainingly of a mysterious nervous illness, which
plunged him into the abyss of melancholy, interfered with
ills creative energy, and constantly distressed him with the
apprehension of a general breakdown. He wrote but
little now, though the cantatas which belong to this
|j)eriod, and the canzonet Ecco quel fiero istante, which he
sent to his friend FarineUi, rank among the most popular
tof his productions. It was clear, as his latest and most
genial biographer, Vernon Lee, has phrased it, that " what
ailed him was mental and moral ennui." In 1755 the
Countess Althann died, and Metastasio was more than ever
reduced to the society which gathered round him in the
bourgeois house of the Martinez. He sank rapidly into
the habits of old age ; and, though his life was prolonged
till the year 1782, very little can be said about it. On
the 12th of April he died, bequeathing his whole fortune
of some 130,000 florins to the five children of his friend
Martinez. He had survived all his Italian relatives.
Durin;^ the long period of forty years in which ^letastasio may be
'almost said to have overlived his originality and creative powei-s
his fame went on increasing. In his library he counted as many as
forty editions of his own works. They had been translated ijito
French, English, German, Spanish, even into Modern Greek. They
had been set to music over and over again by cverj' composer of
distinction, each opera receiving tin's honour in turn from several
of the most illustrious men of Europe. They had been sung by the
>iest virtuosi in every capital, from Madrid to St Petersburg, from
London to Constantinople. The critics of all nations vied iu
raising Mctustasio's credit to the skies. There was not a literary
academy of note which had rot conferred oa him the honour of
membership. Strangers of distinction passing through Vietina
made a point of paying their respects to the old po^t at Jiis lodgings
in the Kohlmarkt Gasse. Letters of congratulation, adulation,
sympathy, respect, condolence, poured iu upon hira. And yet,
during the whole of this lon^ period, he was gradu.iUy outliving tlie
artistic conditions upon which that fame was really founded. It
has "been already pointed out that Metastasio cannot rank as a poet
io the unqualified sense of that word, but as a poet collaborating
^ith the musical composer and perfonaer. His poetry, fui-ther-_
more, was intended for a certain style of music— for the music of
omnipotent vocalists, of thaumaturgical soprani. M'ith the changes
effected in the musical drama by Gluck and Mozart, with the
development of orchestration and the rapid growth of the German
manner, a new type of libretto came into request. Metostasio's
Elays fell into undeserved neglect, together with the music to which
chad linked them. FarineUi, whom ho styled "twin-brother,"
was the true exponent of his poetry ; and, with the abolition of the
class of fingera to which FarineUi belonged, Metastasio's music
suffered eclipse. It was indeed a just symbolic instinct which made
the poet dub this unique soprano nis twin-brother.
The musical drama for which Metastasio composed, and in work-
ing for which his genius found its proper sphere, has so wholly
passed away that it is now difficult to assign nis true place to the
poet in Italian literary history. Compared with Shakespeare, or eve«
with Racine, ho hardly merits the title of a dramatist. Hia inspira-
tion was essentially emotional and lyrical. ' Instead of creating
characters, he created situations for the display of very varied feel-
ings, for all the feelings in fact to which melody allies itself. But
in doing this he showed a capable playwright's faculty. His per-
sonages act and react upon each other. Their characters, though not
in harmony with history or fact, are clearly traced and cleverly sus-
tained. Each of the dramatis personae is an emotion incarnate and .
consistent, admirably fitted for musical effect and contrast. The
clash and combat of passions are vividly presented, with the smallest
possible expenditure of rhetoric, in the dialogues inteaded for
recitative. The climax of emotion is cadenced in appropriate
stanzas, with simple but effective imagery, at the close of each
important scene. The chief dramatic situations are expressed ''jy
lyrics for two or three voices, embodying the several conteii- .ing
passions of the agents brought into conflict by the circumstances of
the plot. The total result is not pure Uterature, but lit^ratur*
supremely fit for musical effect Language in Metastasio's hands is
exquisitely pure and limpid. Of the Italian poets, he professed i
special admiration for Tassoandfor Mariui. But he avoided the con-
ceits of the latter, and wa.s no master over the refined richness of the
former's diction. His ovm style reveals the improvisatore's facility.
Ot the Latin poets he studied Ovid with the greatest pleasure, and
from this predilection some of his own literary qualities may be de-
rived. The pedantic rules of AristoteUan poetics never touched an
artist who felt his real vocation to be the interpretation of music.
For historical propriety, for the psychology of character, for unity of
plot, for probability of incident, he had a supreme disregard. It was
indeed his merit to have discarded all these considerations. His
poetry was the twin-sister of Italian melody, and he was right in
ti^usting entirely to music and action on the stage to render his con-
ceptions vitaL Wkat, therefore, he gained during his own lifetime,
while the musical system to which he subordinated his genius was
yet living, he has since lost when, as now, he must be studied by
readers who have only a faint and dim conception of that perished
art. For sweetness of versification, for limpidity of diction, for
delicacy of sentiment, for romantic situations exquisitely rendered
in the simplest style, and for a certain delicate beauty of imagery
sometimes soaring to ideal sublimity, he deserves to be appreciated
80 long as the Italian language lasts.
There ore numerous editions of Metastasio's works. That hy Calsahlgl, Paris,
1755, 9 vols. 8vo. published under his own superintendence, was the poet's^
favourite. Another of Turin. 1757, and a third of Paris. 1780, deseiTC mention.'
The posthumous worlts were printed at Vienna, 179&. The collected editions of
GenoB, 1802, and Padua. 1811, will probably be found most useful b)- the ceneta]
BUsicnt. Metastasio's life was wiitfen by Alulgi Asslsi, 1783; by Cluiics Burner,
London, 1796 ; and by othei~S) but by im* the most vivid sketch o! hia biography
will be found In Vernon Lee's Sluditl 0/ Iht ISlh Cmtttry la Itnlf. London, l.«SO,
a work which throws a flood of light upon the development of ItAiian dramallQ
music, and upon the place occupied by Metastuslo in the aitlstic movement of tha
last centui-y. ' (J. A. S.)
METCALFE, Chakles Theophiujs Metcalfe, Babojt
(1785-1846), a distinguished administrator, was born
at Calcutta on January 30, 1785; he tvas the second son
of Thomas Theophiltis Metcalfe, then a major in the
Bengal army, who afterwards became a director of the
East India Company, and was created a baronet in 1802.
Having been educated at Eton, where he read extensively,
he in 1800 sailed for India as a WTiter in the service of the
Company. After studying Oriental languages with success
at Lord Wellesley's coUege of Fort William, he, at the age
of sixteen, received an appointment as assistant to Lord
Cowley, then resident at the court of Sindhia ; in 1802
he became assistant in the ofiice of the chief secretary ; in
1803 he was transferred to that of the governor-general,
and in 1806 to that of the commander-in-chief. On August
15, 1806, he became first assistant to the resident at Delhi,
and in 1808 he was selected by Lord Min to for the difficult
post of envoy^to the court of RanjitSinh at Lahore; here,
XVL — .14
106
M E T — M E T
on April 25, 1809, he successfully concluded the important
treaty securing the independence of the Sikh states between
the Sutlej and the Jumna Four years aftom'ards he was
made principal resident at Delhi, and in 1819 he rece;%<;d
the appointments of secretary in the secret and political de-
partment, and of private secretary to the governor-general
(Lord Hastings). From 1820 to 1823 Sir Charies (who
succeeded his brother in the baronetcy in 1822) was resident
at the court of the nizam, but in the latter year he was com-
pelled by the state of his health to retire from active service ;
in 1825, however, he was so far restored as to undertake
the residency of the Delhi territories. Two years after-
wards he obtained a seat in the supremo council, and in
February 1835, after he had for some time been governor
of Agra, he, as senior member of council, provisionally
succeeded Lord William Bentinck in the governor-general-
ship. During his brief tenure of office (it lasted only till
March 28, 1836) he originated or carried out several
important measures, including that for the liberation of the
press, wliich, while almost universally popular, complicated
his relation with the directors at home to such an extent
that he withdrew from the service of the Company in 1838.
In the following year he was appointed by the Melbourne
administration to the governor.sliip of Jamaica, where the
diiBculties created by the recent passing of the Negro
Emancipation Act had called for a high degree of tact and
ability. Sir Charles Metcalfe's success in this delicate
position was very marked (see vol. xiii, p. 551), but unfor-
tunately his health compelled his resignation and return to
England in 1842. Six months afterwards he was appointed
by the Peel ministry to the governor-generalship of Canada,
and his success in carrying- out the policy of the homo
Government was rewarded with a peerage shortly after his
return in 1845. He died at ilalshanger, near Basingstoke,
September 3, 1846. See J. W. Kaye's Life and Corre-
ipomhiKe of Charles Lord Metcalfe, London, 185J
METELLUS, the name of the most important family of
the Eoman plebeian gens CajciUa. They rose to distinction
during the Second Punic War, and NiEvius satirized them.
QuiNTUS CiECiLius Metellus Macedonicus, pra;tor
148 B.o. in Macedonia, defeated Andriscus in two battles,
and forced him to surrender. He then superintended the
conversion of Macedonia into a Koman province. He tried
unsuccessfully to mediate between the Achsan league and
Sparta, but, when the Achreans advanced, he defeated
them easily near Scarpheia ; Mummius soon after super-
Beded liiiu, and returning to Italy he triumphed in 146.
'Consul in 143, he reduced northern Spain to obedience.
In 131 censor with Q. Pompeius (the first two plebeian
censors), he proposed that all citizens sliould be compelled
to marry. He was a moderate reformer, and was con-
sidered the model of a fortunate man ; before his death
in 1 1 5 three of his sons had been consuls, one censor, and
the fourth was a candidate for the consulship.
Qotntus C/Ecilius Metellcs Numidictjs, whoso repu-
tation for integrity was such that when he was accused of ex-
tortion the jury refused to examine his accounts, was selected
to command against Jugurtha in 109 B.C. He subjected
the array to rigid discipline, and aimed solely at seizing
Jugurtha himself; he defeated the king by the river
Muthul, and next year, after a difficult mqrch through tho
desert, took his stronghold Thala. Jlarius, however,
accused Metellus of protracting the war, and received tho
consulate for 107. Metellus returned to Homo and
triiunphed. Saturninus, whom as censor he tried to
remove from the senate, passed in 100 an agrarian law,
inserting a provision that all senators should swear to it
within five days. All complied but Metellus. who retired
to Asia. After Saturninus was killed, he returned, but
died shortly after under suspicion of poison.
Q0iNrcs C^ciiitjs JLetellus Pros, so called from his
efforts to restore his father Jfumidicus, commanded in tla
Social War, defeating Q. Pompa;dinfi | 88 B.C.). SriUa en
departing gave him proconsular command over South
Italy. 'When Marius returned, tho soldiers, who had no
confidence in Octavius, wished Metellus to command, but
he refused. Metellus retired to Africa and afterwards to
Ligiu'ia, resuming his former command on Sulla's return.
In 86 he gained a decisive victory over Norbanns at
Faventia. In Sulla's proscriptions he pleaded in favour of
moderation. . Consul in 80 mth Sulla, he went to Spain
next year against Sertorius, who pressed him hard till the
arrival of Pompeius in 76. Next year MeteUus defeated
Sertorius's lieutenant Hirtuleius at Italica and Segovia,
and joining Pompeius rescued him from the consequencca
of a check at Sucro. From this time Sertorius grew
weaker till his murder in 72. Metellus had previously
set a price on his head. In 71 he returned to^Rome and
triumphed. He was an upright man, of moderate ability.
QuiNTUs Cecilius Meteu.us Pius Scipio, son of
Scipio Nasica, was adopted by the preceding. He was
accused of bribery in 60 B.c, and defended by Cicero. In
August 52 Pompeius pirocured him the consulate. Scipio
in return supported Pompeius, now his son-in-law. On
war being resolved on, Scipio was sent to Syria. His extor-
tions were excessive, and he was about to plunder tha
temple of Artemis at Ephesus when he was recalled by
Pompeius. He commanded the centre at Pharsalus, and
afterwards went to Africa, where by Cato's influence ha
received the command. In 46 he was . defeated at
Thapsus ; in his flight to Spain he was stopped by a cor-
sair, and stabbed himelf. His connexion with two great
families gave him importance ; but he was selfish and
licentious, and his violence di'ove many from his party.
QuiNTUS CECILIUS Metellus Celek, prtetor 63 B.C., was
sent to cut off Catiline's retreat northward. Consul in 61,
his personal influence prevented the holding of the Com-
pitalia, which the senate had forbidden and the tribunes
permitted. He opposed the agrarian law of the tribune
L. Flavins, and stood firm even though imprisoned ; the
law had to be given up. He also tried, though fruitlessly,
to obstruct Caesar's agrarian law in 59. He died that
year under suspicion of poison given by his nife Clodia.
METEMPSYCHOSIS, die transmigration of tho soul,
as an immortal essence, into successive bodily forms, either
human or animal. This doctrine, famous in antiquity, and
one of the characteristic doctrines of Pythagoras, appears
to have originated in Egj^jt. This indeed is affirmed by-
Herodotus (ii. 123) : — "Tho Egji^tians are, moreover, tha
first who propounded the theory that the human soul is im-
mortal, and that when tho body of any one perishes it
enters into some other creature that may be bom ready to
receive it, and that, when it has gone the round of all
created forms on land, in water, and in air, then it once
more enters a human body born for it ; and this cycia of
existence for the soul takes place in throe thoiisand years."
Plato, in a well-known passage of the r/iarlrux, adapts,
as was his wont, t!ie Pythagorean doctrine to his myth or
allegoiy about the soul of tho philosopher. That soul, ha
says, though it may have suffered a fall in its attempt to
contemplate celestial things, stHJ is not condemned, in ita
first entrance into another form, to any bestial existence,
Jjut, according to its attainments, i.e., to tho progre-ss which
it has made in its aspiration for celestial verities, it posses^
in nine distinct grades, into tho body of some one destined
to become a philosopher, a poet, a king, a general, a seer,
(tc. ; or, if very inferior, it will animate a sophist or an
autocrat (rvpan'o;). Plato extends the cycle of existence
to ton thousand years, which is subdivided into periods of
a thousand years, after the Lipse of which the soula undergo
M E T — M E T
1\j7
indgment; and^are admitted to everlasting happiness or
condemned to punishment.^ It is after the period of a
thousand years, he adds, that the human soul comes into
a beast, and from a beast again into a man, if the soul
originally was human.
Pythagoras, who was said to have travelled in Egypt,"
hrought this fantastic doctrine into Magna Grsecia, and
made it a prominent part of his teaching. He declared
that he had himself been Euphorbus, the son of Panthus,
in the time of the Trojan War, and had successively
'inhabited other human bodies, the actions of all which he
remembered.' Closely connected with his theory of metem-
, psychosis was his strict precept to abstain from animal
'food, even from eggs, from some kinds of fish, and (for
'some unknown, probably symbolical, reason) from beans.*
There can be no doubt that the Egyptian custom of pre-
serving the mummies of cats, crocodiles, and some other
creatures had its origin in the notion that they had been
inhabited by souls which might some day claim these
bodies for their own. We cannot suppose that Plato or
the later Greeks reaUy believed in the transmigration of
souls, though there are many allusions to it, generally of a
somewhat playful character. Thus Menander, in the play
'called The Inspired Woman^ (©eot/jopou/ie'r?;), supposes
•some god to say to an old man, Crato, "When you die,
you will have a second existence ; choose what creature
you would like to be, dog, sheep, goat, horse, or man."
To which he replies, " Make me anything rather than a
man, for he is the only creature that prospers by injustice."
Absurd and fantastic as such a doctrine as metem-
psychosis appears at first sight to be, it was in reality a
logical deduction from primitive ideas about the nature of
the soul. It is necessary to explain these ideas (which
have important bearings on other questions) in order to
show that metempsychosis was almost a necessary corollary
to the belief that the soul was the vital or animating prin-
ciple,— that the one distinction between organic and inor-
■ganis was the existence in the former of a i/'i'X'?-
The difference between a dead body and a living body
—or rather, one principal difference— was that the living
animal breathed ; and it was observed that, as soon as the
breath left the body, not only did warmth and motion
cease, but the body began to decay. Life, therefore, was
breath, an opinion tacitly expressed by the Greek and
Roman vocabulary, animus, anima (ave/xo';), tjrvxrj, Trvcv/xa,
spirilus. But breath is air, and air is eternal and imperish-
able in its very nature. Therefore the " soul," or portion
of air which gave animation to the body, did not perish at
the dissolution of the body, but it was returned to the
element of which it was composed, and out of which it
came. It followed that, from the countless millions of
"souls" emancipated from bodies in all time, and still
flitting about invisibly in space, the air must literally
swarm with soul.s, — a doctrme taught by Pythagoras."
Hence, any creature, human or bestial, that fii'st drew the
breath of life, might, so to say, swallow a soul, i.e., take in
vrith the act of respiration the very same particles of air
which had animated some former body. For, although the
soul was air, and returned to its kindred clement, it was
supposed to retain a peculiar character in intelligence
> P. 249 A. Comp. Rev. xx. 2, 13; Viig., ^n. vi. 745, "Doiiec
longa (lies, peifccto teniporis orbe, coDci*et.Tni exeniit labem," &c.
= Diogeu. Laert., viii. 1, 3 ; Luci.-ii, Oaltns, § 18 si;., wliere the
dactriue of metempsychosis and the stories about the pre-existence of
Pythagoras are wittily satirized.
' Lucian, Oall-us, §§ 4, 5 ; Diodor. Sic, x. §§ 9, 10 ; Hor., 0(1 i.
28, 10, " habeutque Tartaia Panllioiden iterum Oreo demissum."
* Qallus, 19, 33. For fanciful reasons for the piohiliition of beans,
, Bee Lucian, Vitarum Audio, § 5. ^ Frag. 222, iVIeineke.
► ° Diogen. Laert., viii. 1, § 32, eTi-oi vdyra riv ie'pA t^uxCi'
(■^/56;);<rts), remembrance of the i)ast, and knowledge and
experience gained in some former existence. Any creature
which first breathed might or mighi, not inhale this or that
soul, just as a net thrown into the water may catch this or
that fish, or no fish at all. But if no " soul ' was inhaled
the creature was believed for that reason to die ; and the
different degrees of intelligence observed in different men
and animals led to the notion that there must have been
a difference in the souls that fii-st animated tlicni. Even
the beUef that the soul, especially near the time of dissolu-
tion from the body, could foreteU future events was based
on the notion of intelligence and c^usciou^uess residtiii"
from experiences of the past.'
As all the science of modern times cannot say precisely
what life is, nor how it fii-st came upon this earth, it is not
wonderful that so obvious, though wholly erroneous, an
explanation should have presented itself to primitive maa
when fii-st he began to incjuire into the causes of things.
The extension of life, by the same term i/'^xv, to plants and
apparently non-breathing things, which, liowever, had birth,
growth, and death, was a development of a philosophic age,
and we are not surprised to find Aristotle recognizing one
form of life as vegetaUe, (Jivtikov.^ The irrational confusion
of " soul " with sentient bodily functions, the attribution to
spirits (tiSoXo) of motion, speech, or other muscular and
material action, though still common, while metempsychosis
is derided or forgotten, is in reality, perhaps, a less excus-
able superstition.
The Romans inherited the doctrine of metempsj'chosis
from Ennius, the poet of Calabria, who must have been
familiar with the Greek teachings which had descended to
his times from the cities of Magna Grxcia. In his Aiumh,^
or Roman hisjory in verse, Ennius told how ho had seen
Homer in a dream, who had assured him that the same
soul which had animated both the poets had once belonged
to a peacock, a story that might seem to indicate Indian
traditions. The Paro Pythayoreus and the Soninia Pytha-
gorea are referred to by Persius and Horace, as well as by
Lucretius.'
Theories suggesting element-worship naturally led to the
notion that air and etlier (upper air) were divine.'" Hence
every soul, as being but a ])ortion of it, was in itself divine,
and therefore immortal. We thus see that the doctrine of
the immortality of the soul, whether attained by a sound
or a vicious course of reasoning, was an inevitable conclu-
sion for early thinkers. Pantheisiu taught that all the
universe was pervaded by a divine mind, and Virgil cites
the opinion of some, that the intelligence of bees was due
to a jiortion of this universal mind residing in them, a view
closely allied to the doctrine of metempsychosis.' ' A di\itie
thing might be polluted, but not destroyed ; hence the
notion of purifying souls by airing them or burning away
a material defilement is enlarged upon by Virgil in tho
sLxth book of the Jineid (724 sq.). (f. a. p.)
5IETE0R, METEORITE. The term meteor, in ad
cordance with its etymology (^crewpos), meant originallj
something high in the air. It has been ap))lied to a large
variety of phenomena, most of them of brief duration,
which have place in the atmosphere. Disturbances in the
air are aerial meteors, viz., winds tornadoes, whirlwinds,
typhoons, hurricanes, &c. The vapour of water in the
atmosphere creates by its forms and precipitations tlie
aqueous meteors, viz., clouds, fogs, mists, snow, rain, hail,
' Diodor. Sic, xviii., § 1. » Ethics, lib. i. 13.
' Pers., Sat. vi. 9; B.or.,' Epist. ii. 1, 52; Lucret., i. 124.
'° S Sros a;e?'jp> Prometheus exclaims, iEsch., P,om., 83.
" Georr;. iv. 219—
His quidam signis, atqne hsec exempla secnti.
Esse apibus partem diviaae mentis ct haustus
.Stherios dixere ; dcum namque ire per omnei
Terrasque tractusque maris cffilumqne profuBdu
108
METEOR
ii-. The effect of liglit upon the atmosphere and its con-
tents caase.-i certain luminous meteors, viz., rainbows, halos,
parhelia, tT\-ilight, mirage, &C. Discussion of all these, and
of like phenomena, belongs to JttETEOEOLOGY (q.v.).
Another class of luminous meteors, known as shooting
or falling stars, fireballs, bolides, ic, have their place in
the upper parts of the atmosphere. But by reason of
thcjir origin from without they, and the aerolites or meteor-
ites which sometimes come from them, belong properly to
astronomy. The term meteor is often used in a restricted
sense as meaning one of these latter phenomena. The
present article will treat of them alone.
The most remarkable of the meteors (and the most
instructive). are those which are followed by the falling of
atones to the earth. These have since the beginning of
the present century attracted so mu«h attention, and the
phenomena have been so frequently examined and described
by scientific men, that they are very well understood. The
circumstances accompanying the fall of stones are tolerably
uniform. . A baU of fire crosses the sky so bright as to be
visible, if it appears in the daytime, sometimes even at
.hundreds of miles from the meteor ; and if it appears in the
night it is bright enough to light up the whole landscape.
It traverses the sky, generally fiuishing its coiu:se in a few
seconds. It suddenly goes out, either with or without an
apparent bursting in pieces, and after a short period a loud
detonation is heard in all the- region near the place where
the meteor has disappeared. Sometimes only a single stone,
sometimes several are found. For some falls they are
numbered by thousands. About three thousand were
obtained from the fall of L'Aigle in 1803, scattered over a
region about 7 miles long and of less breadth. A like
number. was obtained from the fall of Knyahinya on June
9, 1866. At Pultusk a stiU larger number were collected,
scattered over a larger space, by a fall in January 1868.
From the Emmet county (Iowa) faU, May 10, 1879, a
similarly large number have been secured.
These meteors leave behind them in the air a cloitd or
train that may disappear in a few second,s, or may remain
an hour. They come at all times of day, at all seasom? of
the year, and in aU regions of the earth. They come
irrespective of the phases of the weather, except as clouds
conceal them from view.
Let us describe one or two of these meteors more in
detail. On the evening of the 2d of December 1876,
persons in or near the State of Kansas saw, about eight
o'clock in the evening, a bright fireball rising from near
where the moon then was in the western sky. It increased
in brilliancy as it proceeded, becoming so bright as to
compel the attention of every one who was out of doors.
To persons in the northern part of the State the meteor
crossed the southern sky going to the east, to those in the
southern part it crossed the northern heavens. To all it
went down near to the horizon a little to the north of east,
the whole flight as they saw it occupying not over a
minute.
The same meteor was seen to pass in nearly the same
way across the heavens from west-south-west to east-north-
east by inhabitants of the States of Nebraska, Iowa,
Missouri, Wisconsin, Illinois, Michigan, Kentucky, Indiana,
Ohio, Permsyjvania, and West Virginia. But besides this
there were heard near the meteor's path, four or five
minutes after its passage, loud explosions like distant
cannonading, or thunder, or like the rattling of empty
jwaggons over stony roads. So loud were these that people
and animals were frightened. East of the Mississippi
river these e>q)losions were heard everywhere within about
CO miles of the meteor's path ; and in Bloomington, Indiana,
sounds were heard supposed to come from the meteor even
lat a distance of nearly 160 miles from it. Over central
Illinois it was seen to break into fragments like a rocke^
and over Indiana and Ohio it formed a flock or cluster of
meteors computed to be 40 miles long and 5 miles broad.
The sky in New York State was wholly overcast. Persom
in Ohio and Pennsylvania, who from their situation
could look over the cloud last, saw the meteor passing oe
eastward over New York. From many places in the
State itself came accounts of rattling of houses, thimdering
noises, and other liJce phenomena, which at the time wer«
attributed to an earthquake.
At ■ one place in northern Indiana a farmer heard t
heavy thud as of an object striking the ground near hk
house. The ne.\t morning he found on the snow a stone of
very pecidiar appearance weighing three-quarters of a poundj
which from its character there is every reason to believ»
came from the meteor. By putting together the variou*
accounts of observers, the meteor is shown to have become
first visible when it was near the north-west comer of th»
Indian Territory, at an elevation of between 60 and 100
miles above the earth. From here it went nearly parallel
to the earth's surface, and nearly in a right line, to a point
over central New York. Dming the latter part of iti
course its height was 30 or 40 miles. It thus traversed
the upper regions of the air through 25° of longitude and
5° of latitude in a period of time not easily determined^
but probably about two minutes. A part of the body may
have passed on out of the atmosphere, but probably th»
remnants came somewhere to the ground in New Yoil^
or farther east.
A somewhat similar meteor was seen in the evening of
JvUy 20, 1860, by persons in New York, Pennsylvania,
New England, &c., which first appeared over Michigan, at
a height of about 90 miles. The light was so brilliant aa
to caU thousands from their houses. It passed east-soutb-
east, and over New York State, at a height of about 50
miles, broke into three parts which chased each other across
the sky. At New York city it was seen in the nort^^
while at New Haven it was in the south. At both place*
the apparent altitude was well observed, and its true height
proved to be about 42 miles above the earth's surfac*
between the two cities. It filially disappeared far out over
the Atlantic Ocean. It is doubtful whether any one heard
any sound of explosion that came from this meteor, and
no part of it is known to have reached the ground. Th»
velocity was at least 10 or 12 miles per second, or fiftj
times the velocity of soimd. These two meteors wer»
evidently of the same nature as those which have furnished
so many stones for our museums, except that the one was
so friable that it has given us but one known fragment
while the other was only seen to break in two, not even a
sound of explosion being known to have come from th»
meteor.
Next to the stone-producing inelcor is the fireb-Tll, or
bolide, which gives generally a less brilliant light tkan the
former, but in essential appeaiances is like it. The meteor ai
July 20, 1860, above described, though unusually brilliant
was one of this class, and represents thousands of bolides
which have been seen to break in pieces. The bolides
leave trains of light behind them just as the stone meteors
do ; they travel with similar velocities both apparent ant
actual, and in all respects exhibit only such differences erf
phenomena as would be fully explained by differences im
size, cohesion, and chemical constitution of stones causing
them.
Ne.xt to the bolide is a smaller meteor which appeals
as if one of the stars were to leave its place in the heavens,
shoot across, the sky, and disappear — all within the fractios
of a second. Some meteors of this class ore as bright as
Venus or Jupiter. Some are so small that though you look
directly at the meteor, you doubt whether you see one fit
METEOR
109
mot In the telescope still smaller ones are seen that are
■visible to the naked eye. Meteors comparable in bi-ight-
■ess to the planets and the fixed stars are usually called
Aooting stars.
These various kinds of meteors differ from all other
luminous phenomena so as to stand in a group entirely
alone. Though they have been sometimes regarded as
separable among themselves into three or four different
species, and for purposes of description may still be so
divided, yet they all seem to have a Uke astronomical
character, and the differences are only those of bigness,
chemical constitution, velocity, <tc. There appears to be
no clear line of distinction between the stone-producing and
the detonating meteors, nor between those heard to e.xplode
uid those seen to break in pieces, nor between these and
the simple fireballs, nor between the fireball and the
faintest shooting star.
Alliludes of Meteors. — The first important fact about
ihe meteors is the region in which they become visible to
■s. In hundreds of instances observations have been
made upon the luminous path of a meteor at two or more
stations many miles apart. When such stations and the
path arc properly situated relatively to each other, observa-
tions carefully made will show a ijarallax by which the
height of the meteor above the earth, the length and di-
rection of the path, and other like quantities may be com-
puted. The general result from several hundred instances
is that the region of meteor paths may be in general
regarded as between 40 and 80 miles above the earth's
surface. Some first appear above 80 miles, and some
descend 'lelow 40 miles. But an altitude greater than
100 miles, or one below 25, except in the case of a stone-
furnishing • meteor, must be regarded as very doubtful.
,Thus the meteor paths are far above the usual meteoro-
logical phenomena, which (except auroras and twilight)
have not one-tenth of the height of the meteors. But
■with reference to all other astronomical phenomena they
are very close to us. The comets, for example, are well-
nigh a millionfold, and even the moon is a thousandfold,
more distanc from us.
Velocities of Meteors. — When the length of a luminous
path is known, and the time of describing it has been
observed, it is easy to compute the velocity in mOes.
Unfortunately the large meteors, describing long paths,
oome at rare intervals, and unexpectedly, and it is a happy
accident when ope is observed by a person accustomed to
estimate correctly short intervals. of time. On the other
hand, the total time of visibility of the shooting stars,
which come so frequently that they may be watched for,
is usually less than a second. It is not easy to estimate
correctly such an interval, where the beginning and ending
are not marked by something like a sharp cUck. Hence
all estimates and computations of velocities of meteors are to
be received with due regard to their uncertainty. We may
only say in general that the velocities computed from good
observations are rarely if ever under 8 or 10 miles a second,
or over 40 or 50 miles, and that some have far greater
velocities than others. The average velocity seems to be
nearly 30 miles.
W/iat makes the Luminous Meteor. — The cause of a
meteor is now universally admitted to be something that
enters the earth's atmosphere from without, with a
Telocity relative to the earth that is comparable with the
earth's velocity in its orbit, which is 19 miles per second.
By the resistance it meets in penetrating the air the light
and other phenomena of the luminous train are produced.
Under favourable circiunstances, portions of these bodies
jfsach the earth's surface as meteorites.
Meteoroids. — A body which is travelling in space, and
which on coming into the air would under favourable
circumstances become a meteor, may be called a uieteca-
oid.
Tlie meteoroids are all solid bodies. It would hardly ,
be possible for a small quantity of gas out iji space to
retain such a density as would enable it on coming into
the air to go 10 or 100 miles through aven the rare upper
atmosphere, and give us the clear line which a shooting
star describes. Even if a liquid or gaseous mass can travel
as such in space, it would be instantly scattered on striking
the air, and would appear very unlike a shooting star or
bolide.
Kttmbers of Meteors. — Of the larger meteoi-s there are in
the mean six or eight per annum which in the last fifty yeare
have furnished stones for our collections. A much larger
number have doubtless sent down stones which have never
been found. Thus Daubri^e estimates for the whole earth
an annual number of six or seven hundred stone-falls.
But of the small meteors or shooting stars the number,
is very much larger. Any person who shoiUd in a clear
moonless night watch carefully a portion of the heavens
•would, in the mean, see at least as many as eight or ten
shooting stars per hour. A clear-sighted and practised
observer will detect somewhat more than this uunibor..
Dr Schmidt of Athens, from observations made during
seventeen years, obtained fourteen as the mean hourly num-
ber on a clear moonless night for one observer during the
hour from midnight to 1 a.m. A large group of observers,
as has been shown by trial, would see at least six times as
many as a single person. By a proper consideration of the
distribution of meteor paths over the sky, and in actual
altitude in miles, so as to allow for mists near the horizon,
it appears that the number over the whole globe is a little
more than ten thousand times as many as can be seen in
one place. This implies that there come into the aii- not less
than twenty millions of bodies daily, each o£ which, under
very favourable conditions of absence of sunlight, moon-
light, clouds, and mists, would furnish a shooting star
visible to the naked eye. Shooting stars invisible to the
naked eye are often seen in the telescope. The numbers
of meteors, if these are included, would be increased at
least twentyfold.
How detisely Space infilled vntk Meteoroids. — By assuming
that the absolute velocity of the meteors in space is equal
to that of comets moving in parabolic orbits (we have good
reason to believe that this is nearly their true velocity), we
may prove from the above numbers that the average number
of meteoroids in the space that the earth tra v erses is, in each
volume equal to that of the earth, about thirty thousand.
In other words, there is in the average to every portion of
space equal to a cube whose edge is about 210 miles one
meteoroid large enough to make a shooting star bright
enough to be visible to the naked eye. Such meteoroids
would, upon an equable distribution, be each in round
numbers 250 miles from its near neighbours. All these num-
bers rest upon Dr Schmidt's horary number fourteen, and
for a less practised observer and a less clear sky they would
be correspondingly changed. How much they would need
to be altered to represent other parts of space than those
near the earth's orbit is a subject of inference rather than
of observation.
Motion in Space. — The meteoroids, whatever be their
size, must by the law of gravitation have motions about
the sun in the same way as the planets au<J comets, that
is, in conic sectioiis of which the sun is always at one focus.
The apparent motions of the meteors across the sky imply
that these motions of the meteoroids relative to the stm
cannot as a rule be in or near the plane of the ecliptic.
For if they were there, since the motion of the earth is also
in the ecliptic, the motion of the meteoroids relative to .the
earth wQuld be in the same plane. This would inrolve
110
METEOR
that all tlio meteor paths as seen on the sky would if jiro-
duced backward cross the ecliptic above the horizon. lu
fact there is no tendency of this kind. Hence the metcor-
oids d'j not move in orbits that are near the ecliptic as the
jilanets do, but like the comets they may and usually do
hive orbits of considerable inclinations.
Kumbers tlirovjh the Kiyhl. — There are more meteors
Been in the morning hours than in the evening. If the
meteors had no motion of their own in space, the earth
would by its motion receive the meteors only on the bemi-
Ephere that was in front. There would be no meteors seen
in the other hemisphere. On the other hand, if the meteors
had such large velocities of their own as that the earth's
velocity might be neglected in comparison, and if the
<lirectious of the meteors' motions were towards all points
iiidiscriminately, then as many would be seen in one part
of the night as another. In fact there are 'about three
times as many seen in the morning hours as in the evening.
The law of change from evening to morning gives a means
of proving that the mean velocity of meteors is so great
that they must in general be moving in long orbits abo'it
the sun. In this respect also the meteoroids resemble
comets, and are unlike planets, in their motions. Of the
Btone-furnishing meteors more are seen in the day than in
the night, and more in the earlier hours of the night than
du the later. This is probably due to the fact that more
persons are in a position to sec the stone-falls at the periods
of greater abundance.
Star Showers. — While the average number of shooting
stars for a single observer at midnight may be regarded as
tolerably constant, there have been special epochs when
many more have been seen. In certain instances the sky
has been filled with the luminous trains, just as it is filled
by descending snowflakes in a snowstorm, making a
veritable shower of fire. One of the best-observed, though
by no means the most brilliant, of these showers occurred
on the evening of the 27th of November 1S72. Some of
the observers of that shower, counting singly, saw at the
rate of eight or ten thousand shooting stars in the course
of two hours. The distances of the meteoroids in the
middle of the swarm which the earth then passed through,
each from its nearer neighbours, would be 30 or 40 miles.
The following quotations show the impression made by
star showers in times past : —
"In the year 2S6 [of the Hesira] there h.ippened in Egypt an
earthquake on Wednesday the 7tli of Dhu-l-Ka'dah, lasting from the
iiiidJlc of the night until morning ; and so-called naming stars
struck one against nnothci- viiilenrly while being boine eastward
and westward, nortliward and southward, and no one could bear to
look toward the heavens on accfiinit of this iihenomenon."
"lathe year 599 [of the Hegiia], on the night of Saturday, on
the last day of lluhanani, stars shot hither and thither in the
lieavous, eastward and westward, and flew against one another like
ft scatteiiiig swarm of locusts, to the right and left ; people were
thrown into consternation, and cried to God the Most High with
confused clamour."
"These meteors [November 12, 179D] might be compared to tho
blazing eheaves shot out from a firework."
"The Iihenomenon was grand and awful; tho wholo lieavens
iippoared as if illuinin.itcd with sky rockets."
November 13, 1333. "Thick with streams of rolling firej
tcarcely a space in the Cnuaineut that was not filled at every
instant."
"Almost mfiuite number of meteors; they fell like flakes of
snow."
Kovemher Meteors or Leonids. — These quotations all refer
(except possibly the fir.^t) to a shower which has appeared
in October and November of many different years since its
first kno\vn occurrence on the 13th of October 902 a.d.
Dates of these showers are given in tho following table : —
0.t. 13, 902. Oct. 17, 1101. Oct. 25, lCn2. Kov. 13, 1833.
Oct. 15, 931. Oct. 19, 1202. Kov. 9, lC:i8. Nov. H, 1800.
Oct. 14, 934. Oct. 23, 1360. Kov. 12, 1799. Nov. 11, 1SC7.
Oct 15, 1002. Oct. 20, 1633. Kov. 13, 1832. Kov. 14, 1868.
On several years after 1S33, and beiore and aft«
1866-63, there were unusual numbeis of those meteors seen
on the mornings of November 13, 14, and 15, though per-
haps they would have been uimoticed Lad there not beeo
special watching for them. It will be seen that all these
showers are at intervals of a third of a century, that they
are at a fixed day of the year, and that tho day has moved
steadily and uniformly along the calendar at the rate of
about a month in a thou&and years. The change of twelve
days in tho 17 th century is due to the change from old to
new style.
Tlie only explanation of this periodical display that is
now seriously urged, and the one which is universally
accepted by astronomers, is that there is a long thin stream
of meteoroids, each of which is travelling about the sun in
a conic section. These conic sections are all nearly
parallel, and have nearly the same major axis, extending
out about as far as to the orbit of Uranus, and each requir-
ing the common period of thirty-three and a quarter^
years. The length of the stream is such that the most
advanced members are six or eight years ahead of the
hiadermost, and they all cross the earth's orbit with a
velocity of about 26 miles a second. Since the earth
plunges through the group nearly in the opposite direction,
the velocity wnth which, they enter the air is 44 miles a
second. One of the facts which have greatly aided us in
arriving at this explanation is that these meteors in all
the years and through aU hours of the night cross the sky
as we look at them in Unes which diverge from a point
near the centre of the sickle in the constellation Leo ; henca
the paths in the air are parallel. This implies ,that their
velocities relative to the sun are all parallel and equal to
each other. The radiation from Leo has given to them the
name Leonids.
Orbit of the Leonids. — This orbit, common to all the.'
Leonid meteors, is incUned to the ecliptic at an angle of 17
(or rather 163°, since the motion is retrograde), has a major
axis of 10-34, a periodic time'of 3327 years, and a peri-
helion distance a little less than unity.
The above orbit, and that alone, explains the several
appearances of the November meteors, the annual and the
thiity-three year periods, the radiation from Leo, and the
change of day of the month in the course of the centuries.
This it does so completely that the result has never been
questioned by astronomers. Shortly after the publication
by Professor Adams in 1867 of the last link in the chain
of the proof of this orbit, there was also published tho
definitive orbit of the comet 1866 L That the comet was
running almost exactly in the orbit of the meteors was at
once recognized. In fact the comet is itself, in a sense, a
meteoroid, and the principal member, so far as we know,
of the group. Leonids had been seen in 1863, two years
and two months in advance of the comet, while those of
1866 were ten months behind it. Those of later years (a
few Leonids were seen even in 1870) were extended along
the line of tho comet's path behind it. The leaders of this
long file of meteoroids had [lassed up beyond the orbit of
Juiiiter long before those which brought up the rear had
crossed that planet's orbit going do\ra toward the sun.
The thickness of tho stream is less than the ten-thousandth
part of its length. In the densest jiart that we have
recently passed through— namely, that traversed in 1833—
the density of the stream may be expressed by saying that
each meteoroid must in tho mean have been 10 or 20
miles from its nearest neighbours.
Wh(tt males this Comet and these Meteors deseribe lh<
same Orbit about the Sun f— Us path might have been
inclined to the ecliptic at any angle instead of 163 . Or,
n-ith this inclination, its plane might have cut tho earthf
orbit at any other place than where the earth is on the 14th
METEOR
111
of November. Or, happening to have these two elements
in common, it might have passed the earth's orbit nearer
the sun or farther away from it than the earth is. Or,
having these three things in common, it might, by a slight
difference in velocity, have had a periodic time much more
or much less than thirty-three years. Or, with all these
in common, it might have crossed the earth's orbit at a far
different angle than the meteors. These several independ-
ent elements for the comet and the" meteors are substan-
tially identical, and this identity proves almost beyond
doubt that between the two either there is now an actual
or else there has been in the past a causal connexion.
pTiat there is now any physical connexion is thovoaghly
[disproved by the immense magnitude of the stream, and
by the isolation and distances from each other of the
individual components. It seems difficult to find any cause
that should bring into such a strangely shaped group
bodies that had originally orbits distributed at random.
Hence we are apparently forced to conclude that these
meteoroids have something common in their past history.
In fact they seem to have been once parts of a single body,
and these common elements are essentially those of the
parent "mass. By some process not yet entirely explained
they have become separated from the comet, thrown out of
the control of its attractive power, and so left to travel
each one in its o^vn orbit. If the cause of separation was
not too violent, each new orbit would necessarily be but
slightly different from that of the comet. Very small
variations in velocity, and hence in periodic time, would
in the course of ages scatter the several individuals along
the orbit even to the length of many hundreds of millions
of miles.
Tlie Meteor Group is not the Cornelia Tail. — These
meteoroids must be carefidly distinguished from the
comet's tails. The former follow or precede the comet
exactly in the comet's path; the particles that compose
the latter are driven oS by the sun's repulsion directly
away from the comet's path. The meteoroids and the
comet have orbits with nearly common elements ; the
orbits of the particles of the tail have elements that are
unUke each other, and unlike those of the comet. The
meteoroids are undoubtedly solid masses ; the tails are
pulverulent or gaseous.
Twin Comets of 1366. — The comet 1866 I. is probably
not the only one that has been connected with the November
meteors. In 1366, a few days after the earth went through
the meteor stream, a comet appeared in the northern
heavens, and, passing directly in the hne of the stream so
close to the earth as to describe an arc of 90° in a single
day, disappeared in the constellation Aquarius. Immedi-
ately upon its disappearance a second comet was seen in
the north, which followed nearly in the same path. The
Chinese accounts are not sufficiently exact to furnish
independent orbits for them, but both comets were
undoubtedly members of the Leonid stream. The comet
1866 L may be identical with one of them.
The AndroTncds and Biela's Comet. — Mention has been made of the
star shower of November 27, 1372. The periodical comet known
.13 Biela's, which makes three revolutions in twenty years, passes
very near the earth's orbit at a longitude corresponding to
November 27, but by reason of its direct motion the node has
had considerable motion in longitude as the result of perturbations,
ileteors having the same orbits as Biela's comet would have a
radiant in the constellation Andromeda, that is, would cross the
sky in lines diverging from a point in that constellation. They
might, however, be at dates after or even before November 27.
Unusual numbers of meteors were seen December 7, 1793, by
■Brandos. A like abundance was seen Deeember 7, 1838 ; and, as
they had beeu expected, and radiation was now looked for, they
jwere found to diverge from a point in Andromeda. Hence they
Save been called Andromeds. Since 1852 Biela's comet itself has
been entirely lost. The star shower of November 27, 1872,
frevioDsl^ referred to, had a radiant in Andromeda, and in every
way appeared as though its meteors' had once been parts of Biela's
comet. A sprinkle three d.ays earlier, on the night of November
24, had the same radiant, and came from a less dense outlying
parallel stream. A small comet was seen in the southern sky by
Pogson in the dircctiou opposite to the radiant shortly after tlio
shower. Biela's comet had been found in 1845-46 to be in two
parts, which at its next return to perihelion in 1852 had separated
to eight times their foraiiir distance. But the meteor streams of
1872 could hardly have been separated from the comet so recently,
and the Pogson comet if of the same origin must also have left tha
parent mass at an earlier date than 1845. No ordinary perturba-
tions would in a short period have so changed the orbits. The
parts of the small stream traversed by the earth, December 1838 and
December 1798, were far from the comet, and these fragments muii
have been thrown off much earlier.
The fcrxids and the Comet 1862 III.— There is a third epotli
when meteors appear in unusual numbers, viz., the 9th to 11th ol
August. This "sprinkle," as it may be called, has been seen cou
stautly at the time named for nearly fifty yeai-s, and there art;
on record accounts of similar appearances in the earlier years befoie
its annual character had been discovered. Some observers have
thought that there were evidences of a variation having a long
period, but the proof seems as yet unsatisfactory, and the display
may be regarded as tolerably constant from year to year. On every
10th of August we may confidently expect a display of meteors that
shall be at least four or five times as numerous as those of ordinary
nigbts. The radiant is in the constellation Perseus, and hence the
name Perseids.
The comet 1862 III., which has a period of more than a hundred
years, passes close to the earth's orbit, nearly cutting it at the place
of this shower, and has a velocity and direction corresponding to
this radiant. Hence a connexion of the Perseid meteors with this
comet is presumed, like that which the Leonids and Andromeda
have with the comet 1866 I. and Biela. The meteors are distri'
buted along this orbit more regularly than .along either of the othei
two, and at the same time the breadth of this group is a hundred
times greater than that of the Leonids. We must for the present
regard it rather as a meteor ring, the meteoroids being scattered
along the entire conic section whicb the comet describes. This ring
has an inclination of 113° with the ecliptic.
Meteors of April 20-^21 — Lyraids.—Ahont the 20th of April there
have been several qiute biilli.int star showers, the earliest on
record having been in the year 687 B.o. On that day meteors have
been observed which radi.itcd from L^tti, and to these the name
Lyraids has been given. The comet 1861 I. p.nsses neat th^ earth's
orbit in that longitude, and any meteors having such a connexion
witb it as is proved for the Leonids with comet 1SC6 I. would also
radiate from Lyra.
Again, at several other periods of the year, meteors have been
seen in unusual nimibers which seem to be connected with certain
comets. •
Meteor Radiants. — We have thus definite proof that the
earth at certain epochs plunges through meteor streams,"
and that these streams travel along the same track as cer-
tain comets. The question is at once asked— Do not the
sporadic meteors, those which are seen on any and all
nights of the year, belong to similar streams 1 An immense
amount of labour has been spent in observing the paths of
meteors, and classifying them, so as to detect and prove the
existence of radiant points. As many as a thousaud sudi
radiants have been suggested by the different investigators.
Some of these are duplicates, some wiD prove to be acci-
dental coincidences ; .but a goodly number may reasonably
be expected to endure the test of future observations
Such will show the existence of meteor streams, and per
haps will be comiectod with comets that are now known,
or that may hereafter be discovered.
The radiants have been spoken of as if thej were points
in the heavens. This is so nearly true as to justify all the
conclusions that have been deduced above. But in fact a
radiant, even in the star showers in which it is most
sharply defined, must be regarded as a small area. The
apparent meteor paths when produced backward do not
exactly meet in a point. If. they be treated as proceeding
from a small area, it does not appear that this is a long
narrow one. Hence it may be shown that the paths of
the meteors in the air are not exactly parallel either to a
line or to a plane. This can hardly be due to a want of
parallelism of the paths before the meteoroids meet the
earth, but is rather due to their glancing as they strike the
ri2.
M E T E 0 K
air." These facts add not a little to the diiBculties to be
overcome by the energetic observers and investigators who
are trying to deduce order out of an apparent chaos.
Meteorites. — The fragments which fall immediately after
the di.sappearance of large meteor.s have been carefully
collected and preserved in mineralogical miLscums, and have
been studied with special interest. The largest coUectious
in Europe are in Vienna, Paris, London, and Berlin, some
of these representing over three hundred localities. , In the
United States there are large collections at New Haven,
Amherst, and Louisville.
In several respects these fragments differ at first sight
from terrestrial rocks.
They are when found almost always covered in part or
entirely with a very thin black crust, generally less than
'^\f of an inch in thickness. This crust may have a bright
lustrous svu-face, or it may be of a lustreless black. It has
evidently been melted, yet so rapidly as not to change in
the least the parts of the stone inomediately adjacent.
Streaks showing the flow of the melted matter are often
seen on the sm-face. Upon some surfaces are what appear
to be deposits of the melted matter that has flowed off from
the others. Some siu^aces are only browned, showing an
apimrently recent fracture, and some cracks are found in
stones which are not yet completely broken in two.
The surfaces very often have small cup-like cavities,
sometimes several inches in diameter, sometimes like deep
imprints in a plastic mass made by the ends of the fingers,
and sometimes stiU smaller. These " cupules " have not
only various sizes in different stones, but even in the same
stone differ considerably from one surface to another. They
appear in meteorites that are almost exclusively iron, as
^well as in those mainly destitute of that metal, and they
may be regarded as a characteristic of meteorites.
The meteorites have usually metallic iron as one of their
component parts. Native iron is very rare indeed among
ten-estrial minerals, and its presence in the meteorites is
therefore characteristic. Sometimes the iron forms the
principal part of the body, giving it the appearance of a
mass of that metal. Sometimes it forms only a connected
framework whicli is filled in with mineral matter.. Some-
times particles of iron are scattered through a stony mass ;
and a few meteorites are said to be destitute of metallic
iron altogether. The metallic iron is always accompanied
with nickel.
The stony meteors when broken or cut through have
usually a greyish interior, and often exhibit a peculiar
globukr structure. From the small romaded grains that
give it this appearance, the name chondrite (from p^oiSpos,
a ball) has been applied to this kind of meteorite. Some-
times the irregular fragments are compacted into a kind of
breccia.
The pieces as we find them are always apparent frag-
ments of some larger mass, and there is no structui-al
appearance which would indicate that the mass might not
be a fragment of a stdl larger one. In some of the faUs
fragments picked up at a distance of miles from each other
fit together in their simply browned surfaces, showing that
|they were true fragments recently seimrated. In some
cases surfaces of the stones are partially polished. In some
'a cross section of the stone exhibits thin black lines as
though the melted matter of the surface had been forced
into the crevices of the partially broken stone.
The stones when seen to fall, if at once picked up, are
usually too warm to be taken in the hand. But cases are
on record in which the stones were excessively cold. They
sometimes, on striking the ground, penetrate into it from 1
to 3 feet. In extreme cases largo ones have struck much
deeper into soft eartli. Sometimes they are broken to
pieces by the impact with the hard earth.
The stones are usually not very large. Although the
light of the meteor is such as sometimes to be seen over a
region 1000 miles in diameter, and the detonation gives
phenomena suggestive of an earthquake over many counties,
yet a stone exceeding 100 lb is quite exceptional in our col-
lections. The total weight socui-ed at any fall has rarely if
ever amounted to a thousand pounds. The average weight
of nine hundred and fifty perfect specimens of the Pultusk
ffll in the Paris museum is 67 grammes, or less than 2J
oz. One of the Hessle meteorites in the Stockholm museum
weighs less than 1 grain. Many of the Emmet countj' mete-
orites (May 10, 1879) are not much larger, though the
largest specimen of that faU weighs nearly 500 lb.
Meteors traversing the Atmosphere. — We can now get a
very good idea of the history of that part of a meteorite's
life between its entrance into the air and its arrival at the
earth. It is entirely invisible untU it has reached that height
at which the density of the air is enough to create con-
siderable resistance. Up to that time it moves almost
exclusively in obedience to the sun's attraction. Tha
earth's attraction may be neglected, especially during the
passage through the air. Since the velocity is a hundred
times that of soimd, the elasticity of the air- is impotent to
remove it from in front of the meteorite, or to prevent a
high degree of condensation. Perhaps the air is liquefied
immediately in front of the stone. Heat is developed in it
enormously, and the stone being pressed closely against the
hot air is melted, with an intense light. The condensed air
charged with the melted matter is pushed aside, and left
behind nearly in the wake of the meteor to form the train.
The brightness of the train rapidly diminishes behind tha
meteor, so that the light of the meteor and the train, modi-
fied by irradiation, make the whole appear to a distant eye
of the shape of a pear or candle-flame. The stone being a
poor conductor of heat, and itself rigid, is not heated in tha
interior either by condensation or conduction, and '^a.y,
reach the ground with its surface only heated, while the
interior is as cold as it had been out in space.
If the stone is a small one it will soon be used up by]
this' intense file. UntU its front surface is rounded by the,
flame, the irregular resistances may cause such a stone toj
glance. But if the stone is larger it \y\Q lose velocity less
rapidly. As it comes do'rni into the i-egion where the air.
is more dense, it will in spite of loss of velocity meet greater
resistance. The aii- pressed hard against it burns it un-.
equally, forming cupides over its surface. The pressure
of the air craclcs the stone, — perhaps scaling off small frag-
ments, perhaps breaking it into pieces of more uniform
size. In the latter case the condensed air in front of the
meteor being suddenly relieved will expand, giving the
terrific explosion which accompanies such breaking up. In
either case a fragment may have still velocity enough to
burn on for an instant in its new path and then come'
invisibly to the earth, covered with a coating, the greater,
part obtained after the principal explosion. In the latter:
part of the coui'se the original velocity has almost all dis-'
appeared, so that the sound travbls faster than the meteor.;
The air's resistance exceeds the earth's attraction, and tha
stones strike the ground only with the force of a spent
cannon ball. It is no doubt in violent disruption that some
of the fractures are made in such a way as to give the
rubbed and polished surfaces.
Trains of Meteors. — The smaller meteors generally have
no perceptible train. Only in exceptional cases do the
trains of ordinary shooting stars remain visible longer than
a fraction of a second. An unusual number of the Leonids
have a bluish train. But the brighter shooting stars and
the larger meteors sometimes have trains that endure for
minutes, and in extreme cases for an hour. Such trains
are at first long narrow lines of light, though much shorter
METEOR
113
i
llan the tracTi of the meteor. They begin at once to
broaden in the middle and to fade away at one or both
ends. Presently they become curved, sometimes with two
or three convolutions. The white cloud floats slowly away
among the stars, coiling up more and more, and finally
fades, out of sight. The cause of all this seems to be as
follows. The heated air -charged with the debris of the
meteor is by the meteor's impact driven off horizontally,
causing the narrow train to spread jnto a doud. The
currents of air differing in direction at different altitudes
twist the cloud into its varied fantastic forms. Attempts
to obtain the spectrum of t)ie trains have been made, and
sodium and magnesium lines have been thought to be
detected in them. The observation, however, is one that
is not easy to make or confirm. The trains have often
colours other than white, and in the case of the brighter
meteors different colours are seen in the different jjarts of
the train.'
Magnitude. — Some'COmputations have been made of the
size of the shooting star meteoroids from the mechanical
equivalent of the light developed by their disintegration.
If all the energy of the meteor is changed into light, then
these 'computations would be conclusive. But a part is
spent in disintegrating and burning the stone, a i«rt
in heating the air, and a part in giving direct motion to
portions of air. ' A computation based on the light develo]icd
gives only a lower limit to the size.
It seems probable that the larger meteors might be safely
regarded as weighing on entering the air only a few
hundreds or at most a few thousands of jKJunds. The
smallest visible shooting stars may be equal in size to
coarse grains of sand, and still be large enough to furnish
all the light exhiUted by them. " The large.ft shooting
stars furnish matter enough to fill with thin trains
cubic miles of space, but this. need not require a very
large tnaas..
J/rfcoricir<mi.— There have boon founil at various times on the
snrface of the earth m.-issea of metaliio iron combiued with niekel.
These have been so like the irons whii-h have been known to fall,
both'in .their structure nnd in coniiK>sition, that they have been
without hesitatioH el.tsscil among the meteoric irons. A maAs of
this 'character weighing 1635 lb, found in Texas, is in the Yale
College .JtiiscuTO. Tlie Cliarcas (llexiro) iion in tlio Paris mu.vum
IS about tlic same size. A ring-shnpcj ma."ia somewhat aiiallrr,
froD) Tuczon," is iiy the Ujiited ■istntes National Museum in
Washington.^ ,A still larger mass is in the British lluscun), and
many*other_.large masses are in public collections or private
{loascssion.
]f^idmaiinsthtUn\ Pi0ures. — If in any of the meteoric irons, whether
seen to fall or found on the earth, a section is cut and ijolished and
then*',etchcd with acids, > aeries -of peculiar lines are developed
which 'are. known as^Widniannstitten figures. The lines of iron
unattatked by the acid consist of an irregular grouping of parallel
rulings' often lying along the fares of a regular octahedron. The
'exhibition "of these figures and the combination of iron with nickel
have been usually considered conclusive evidence of the meteoric
prigin of any iron mass
ificJul Iron of Ovl/ak.-^ir> 1870 Baron Nordenskiold, in his voyage
to Grccnlan<1, found on the shore of the island of Disco fifteen iron
muses, the largest of which weighed 20 tons, all in an area of half
macre.^ ,In the ba&iltic rocks not far distant other iron masses
were found embedded in the basalt -The presence of nickel with
the 5ron,\and the development of lines like the Widmannstitteo
figutw, w^re at once accepted as proof of their meteoric origin, in
spite of the combination with basalt. A more complete examitta<
tion ha.Sf however, established tlie terrestrial origin of these irons,
nr.d gi][eli reasons to hojie for new discoveries of relations existing
between th.r-eaith and the meteors. The additional discovery
of small particloa of metallic iron in dertain otlier igneous rocks-
fcoveajthat the union of the Ovifak irons with bnsalt is not excep-
tional.
Chfmicai' Constitiitiojt «/ Hi ircUoritcs.—tlo neiW element has
teen found in the meteorites. Three elements most widely distri-
buted and most important among the meteorites — iron, silicon, and
oxygen— are also most abundant in our earth., Daubrce gives the
following lists .of elements, arranged eomewh'at jm the degree of
dieir' |import«nce, in meteorites (Maskelvne adds lithium and
iuitiiaon{>^ —
1&-7
Iron.
Titanium.
Magnesium.
Oxygon.
Nickel.
Cobalt.
Tin.
Copjier.
^Aluminium.
Potassium.
Sodium.
Chromium.
Calcium.
Arsenic
Pbosphonia>
Nitrogen.'
Sulphur.
Chlorine^
Carbon.
Hydrogen.
J^laiigane;^.
Afiticrals ifi Mrtcoriies. — Among the minerals in the meteorites
there are several which occur in the rocks on the earth. Amonj;
thcw? are cited by Daubree i^ridote, pyroxene, enstatite, triclinlc
felsmr, chroniite, maguetic pyrites, iron oxide, graphite, and
probably water. Several minerals, however, are found which, so
far as now known, are [fficuliar to the meteorites ; — metallic nickel-
iron, phosphide of iron and nickel (schreibersite), sesquisulphide of
chromium and iron (daubrt'elitc), sulphide of calcium (oldhamite),
and chloride of iron (lawreiicite).
Meteorites of different falls are in general unlike ; but tliere are
many instances in which the stones of two falls are so similarly
constituted that it is not easy to distinguish them.
In four falls (Alais, Cold Bokkeweld, Kaba, and Orgeuil) the
stones contain little or no iron. Iri thes6 carbon appears not as
gr(^,pIiito but in uuiou with hydrogen and oxygen, and also with
soluble and even deliquescent saline matters. The combination!
are aiich as to suggest the existence of humiis and organic remains.
But after careful search nothing of this kind has been detected in
them. In general the meteorites show no resemblance in their
mechanical or mineralogical structure to the granitic and surface
rocks on the earth. One condition was certainly necessary in their
formation, viz., the absence of free oxygen and of enough water to
oxidize the iron and other elements. Perhaps it is to this fact that
aro due tho resemblances between tliese minerals and those of the
dcop-soated rocks of tho earth in tbe formation of which free
oxygen and water were also not present.
Qays in ifetcoritrs. — The meteoric stones . and irons ^hen
reduced to fine particles and placed in the vacuum of a Sprengel air^
pump give off small quantities of gases which may be reasonably pre-
sumed to have been occluded by tiie irons at some time in their earliei
history. Professor Graham found hydrogen in meteoric irons.
Professor Wright has shown that a moderate heat drives off from
tlie stony meteorites carbonic arid and carbonic oxide with a
small amount of hydrogen. Astljo heat increases the pronoi-tion ot
hydrogen (and even some nitrogen) increases till at a full rea heat tho
hydrogengivenotfisby far the largest irortion. From the irons Mmilar
gases aro given off, but the carbon comjxjunds are not so large a
comjioncnt as hydroj^en. The sjtoctra seen in tbe tails of comets arc
not strikingly like those of any of theso ga-vs. But it is impossible
to reproduce in the laboratory tlie conditions under which the
matter of comet's tails is giving off its light. AVe cannot therefor*
aay that these gases may not be the important parts of the coinctic
coma and tails.
Mrtcoroid as Part of a Comrt. — Assuming that the meteorite and
metcoroid once formed an integral jwirt of a comet, not a little
information is given us of the nature of this mystcrions body.'
There is room also for speculation.
First, the tfomet may Iw a single hard body which comes from
the cold of spnco into the heat of the sUn, and there has frag-
ments broken off, just as a stono is shattered in a hot fire. The
nucleus of some of the comets must be very small because invisible
in the telescope, and an impulse that would raise a stone on th<
earth only a k\v inches would eend it permanently away from su .h
a comeL The exposure of new surfaces to the heat of the suu might
give occasion for tho development of gas to form the comet's tail.
Or, secondly, the comet may be a tolerably compact aggregation o(
small boilics not in contact, each one being of the size of a
metcoroid, and kept near to the rest, not by cohesion, but by their
combined attraction. The total mass being small, some membei^
of the gi'oup near the comet's perihelion passage can be by the sun's
perturbing action thrown out into orbits quite icideiiendent of the
comet itself, and yet such as relative to tlie sun shall resemble that
of the main group. Perturbations resembling tidal waves mi-'ht 1>«
preparing other members to be cast off at the next perihelion
passage of the comet.
In either case, If we suppose, as seems probable, fliat the couiot
came from outside the solar system, and that a disturbance by a
large planet changed the original hyperbolic orbit into an ellipse,
the colnet must have passed that planet as a very compact group, i(
not in rf single mass, else the disturbance that changi-d the orbit
would have scattered the group beyond the power of a future recog-
nition of the common origin of the fragments.
}totcoroids as Fuel of the 5»ft.— The idea has been held by
distinguished physicists that the meteoroids in fallijig into tho
sun f\imish by their concussion a supply for the heat which the
sun is constantly sending off into space, — that they are iix fact the
fuel of the sun. ' . Such a view, however, receives but little support
from facts which we know about inete<H"s. The meteoroids of the
August .and .two -Koveniber - Deiiods are evidently permanent
114
M E T — MET
roember-i of the sol.ir syitoni moving in closed orbits. The aanie is
by inference hifjhiy probable for most of the other meteoroids, and
may be true of all of them. Permanent members of the solar
system, however, if tht-y ever fall into the sun, do so only after along
period of perturbation. If any meteoroids come from stellar spaces
and have any uniform or random distribution of velocities or direc-
tions, only a very small portion of these would hit the sun's surface.
The far greater portion would go on in hyperbolic orbits. But
the earth receives the impact of its portion of these foreign
meteoroids, both in their inward and outward course, and in
addition encountei-s a full rhare of the permanent members of the
solar system, of which the sim receives very few or none. It is
not hard to sliow that a supply of meteoroids to the sun sufficient
to make good its daily loss of heat would require that the twenty
million meteoroids which the earth daily encounters, even if aU were
from stellar space, should have an average weight of hundreds of
tons. The facts do not warrant the admission of any such magni-
tude even for the larL^c meteors, much less for the ordinai-y and
small shooting stars. Whatever be the source of the sun's heat,
all the meteoroids of which we know anything are totally inade-
quate to supply the waste.
The literature of meteors and meteoroids is very muclt scattered.
It is mainly contained in the scientific journals and in transac-
tions of learned societies. The series of' -valuable Reports of the
Lnminous Meteor, Committee of the British Association contains
not only the record of an immense amount of original observations.
but also year by year a digest of most of the important memoirs.
Meteoric science is a structure built stone by stone by many
builders. In this article no attempt has been made to assign to
each builder the credit for his contribution. (H. A. N.)
METEORA, a remarkable group of rock-built monas-
teries in Thessaly, in the northern side of the valley of the
Peneus, not quite i^O miles north-east of Trii.'cala, and in
the immediate vicinity of the village of Kalabaka, Stagus,
or Stagoi (the ancient /Eginium). From the Cambunian
chain two vast masse-s of rock are thrust southward into
the plain, surmounted by a number of huge isolated columns
from 8.5 to 300 feet high, '" aoa\i; like gigantic tusks, some
like sugit-loaves, and some like vast stalagmites," but all
consisting of iron-grey or reddish-brown conglomerate of
gnei.ss, mica-slate, syenite, and greenstone. On the summit
of these rocky pinnacles — accessible only by aid of rope
and basket let down from the top, or iu some cases by a
series of almost perpendicular ladders climbing the cliff to
the mouth of a tunnel — stand the monasteries of Meteora
(to McTc'tupa). At one time they were twenty-four in
number; but Holland (1812) and Hughes (1814) found
them reduced to ten; at Ciu-zon's visit (18.34) there were
only Beven ; and in 1853 not more than four c^f these were
inhabited by more than two or three monks. Meteora par
excellence is the largest and perhaps the most ancient. The
present building was erected, according to Leake's reading
of the local inscription, in 1388 (Bjornstuhl, the Swedish
traveller, had given 1371), and the church is one of the
large:>t and handsomest in Greece. St Barlaam's and
St Stephen's (the latter founded by the emperor John
Cantacuzene) are next in importance. The decorations of
the churches contain a large amount of material /or the
history of Byzantine art, not much inferior in value to the
similar treasures at Athos.
Unless the identification with the Ithome of Homer be a sound
one, there is no direct mention of the rocks of Meteora in ancieut
literature, and Professor Kriegk suggests that this may simply b«
due to the fact that they had not then taken on their present re-
markable form. .5i!ginium, however, is described by Livy as a
strong place, -and is frequently mentioned during the Roman wars;
and Stagus appears from time to time in Byzantine WTiters.
See Holland, Travels in the Ionian Ules, &e., 1815; Huplies. Travels in Qreett
and Albania, 1830 ; Curzon, risiV (o MMaHeries in Itie Leranl. 1819 ; Leake, *»•
l.tei-n Oreeee; Professor Krieek In Zeittehr. f. allg. Erdk., Berlin, 1848; T««»
Jiesearc/tes in {lie Jii'jti!an<ts of Tarktf, 18()».
METEOROLOGY
METEOROLOGY, in its original and etymological
scn.se, iilcluded within its scope all apijearances of
the sky, astronomical as well as atmospherical, but the tenn
is now re.'itricted to the de.scription and e.^iplanation of the
phenomena of the atmosph>.ie which may be conveniently
grouped under weather and climate, 'These phenomena
relate to the action of the forces on which the variations
of pressure, temperature, humidity, and electricity of the
atmos[)here depend, but in an especial sense to the aerial
movements which necessarily result from these variations.
In the more exact develojnnent of meteorology, the
scientific investigation of climate long preceded that of
weather. Humboldt's work on Isothermal Lines, published
in 1817, mjust be regarded as the fli-st great contribution
to meteorological science. The importance of this inquirv
into the elistribution of terrestrial temperature if is
Bcarcely possible to overestimate, for, though the isothei-mals
were neces.sarily to a considerable extent hypothetical,
there cannot be a doubt that they presented a first sketch
of the principal climates of the globe. Dove continued
and extended the investigation, and in his great work Oii
tlie Diflril/uiion (if Henl on the Svrface of the Olohe, ]iub-
lished in 1852, gave charts showing the mean temperature
cf the world for each month and for the year, together witli
charts of abnormal temperatiu-e. To this, more than to
any other work, belongs the merit of having popularized
the science of meteorology in the best sense, by enlisting in
its service troops of observers in all parts of the civilized
world.
In 1868 another series of important charts were pub-
lished representing by isobaric lines the distribution of the
mass of the earth's atmosphere, and by arrows the prevail-
ing winds over the globe for thu months and the year.
By these charts the muv<i!a;Hts of the atmosphere and the
immediate causes of these movements were for the first
time approximately stated, and some knowledge was
thereby attained of some of the more diiEcult problems of
meteorology. It was shown that the prevailing winds are
the simple result of the relative distribution of the mass
of the earth's atmosphere, in other words, of the relative
distribution of its pressure, the direction and force of the
prevailing winds being simply the flow of the air from a
region of higher towards a region of lower pressure, or from
where there is a surplus to where there is a deficiency of
air. It is on this broad and vital princijile that meteorology
rests, which is found to be of universal application
throughout the science, in explanation, not onlj' of prevail-
ing winds, but of all winds, and of weather and weather
changes generally. One of the more important uses of the
principle is in its furnishing the key to the climates of the
different regions of the earth ; for climate is practically
determined by the temperatiu'e and moisture of the ■ air,
and these in their turn are dependent on the prevailing
winds, which are charged with the temperature and
moisture of the regions they have traversed. The isobaric
charts show further that the distribution of the mass of
the earth's atmosphere depends on the geographical distri-
T'Ution of land and water in their relations to the sun's
heat and to radiation towards the regions of space in
different seasons.
In 1S82 Looniis published a map showing the mean
rainfall of the globe. This map and others that have been
constructed for separate countries show conclusively that
the rainfall of any region is determined by thf jirevailing
winds considered in relation to regions from which they
have come, and the physical configuration and tomiieraturo
of the jiart of the earth's surface over which they blow.
Tii3 maximum rainfall is jirecipitated bv winds which.
aiUBNAl. rHENOllENA.]
b.'iving traversed a large breadth oi ocean, come up against
and blow over a mountainous ridge lying across tlieir path,
and the amount deposited is still further increased if the
winds pass at the same time through regions the temper-
ature of which constantly becomes colder. On the other
hand, the rainfall is unusually small, or nil, when the pre-
vailin" winds have not previously traversed some extent
of ocean, but have crossed a mountain ridge and advance
at the same time into lower latitudes, or regions the
temperature of which is markedly higher.
While the observational data for the determination of
the geographical distribution of the prime elements of
climate, viz., the pressure, temperature, moisture, and
movements of the atmosphere and the rainfall were being
slowly but surely collected, the great importance of the
.study of weather came gradually to be recognized.
Additional impetus was given to this branch of study from
its intimate bearings on the eminently practical question
of storm warnings. Synchronous weather maps, showing
the weather over a considerable portion of the earth's
surface, were constructed, and some advance was made in
tracing the. progi'ess of storms from day to day. Unques-
tionably one of the first problems of meteorology is to
ascertain the course storms u.sually follow and the causes
by which that course is determined, so as to deduce from
the meteorological phenomena observed, not only the
certain approach of a storm, but also the particular course
that storm will take. The method of practically conduct-
ing this large inquiry in the most effective manner was
devised by the genius of Leverrier, and begun to be carried
out in 18.58 by the daily publication of the BvUelin Inter-
national, to which a weatlier map was added in September
1863. This m'^\i showed graphically for the morning
of the day of publication the atmospheric pres.sure, and
the direction and force of the wind, together \nth tables
of temperature, rainfall, cloud, and sea disturbance from a
large number of places in all parts of Europe. From such
■weather maps forecasts of storms are framed and suitable
Tvarnings issued ; but above all a body of information in a
veiy handy form is being collected, the careful study and
discussion of which is slowly but gradually leading to the
issue of more exact and satisfactory forecasts of weather,
and to a juster kno\iledge of these great atmospheric move-
ments which form the groundwork of the science.
The most cursory glance is sufficient to show that the
ever-changing physical phenomena with which it is the
business of meteorology to deal are all referable to the
action of the sun, it being evident that if the sun were
blotted out from the sky a cold lifeless uniformity would
rapidly take possession of the whole surface of the globe.
Meteorological phenomena naturally group themselves into
two great classes, — those dependent on the revolution of
the earth on its axis, and those dependent on its revolution
round the sun taken in connexion with the inclination of
its axi.s to the plane of its orbit. The science thus divides
itself into two great divisions, the first comprising dinmal
phenomena and the second annual phenome
DiUKXAL Mabch of Phexomexa.
Temperature. — Of the daily changes which take place
in the atmosphere, the first place must be assigned to those
Ti'hich relate to temperature, seeing that on these all other
changes are either directly or indirectly dependent. Obser-
vations of the temperature of the air are therefore of the
first importance in meteorolog)'. A perfectly accurate
i'ljservation of the temperature of the air is unquestionably
laiong the most difficult to make of aU physical observations,
the difficulty being to eliminate the effects of radiation of
suAounding objects. The nearest approach yet made to
the solution of this important problem of physical inquiry
M E T E 0 Ft 0 L 0 a Y
115
was made by Dr Joule in a communication to the
Philosophical Society of Manchester (November 26, 1867,
Proc, vol vii. p. 35). But the manipulative skiU and
time demanded by the method there detailed render it quite
unsuitable for general adoption anyivhero in collecting the
observational data required in the determination of this
important element of climate. It is therefore necessary to
fall on some method which, while it gives results that can
only be regarded as approximate, secures the essential
element of uniformity among the observ-ations.
Fig. 1 represents Stevenson's louvre-bearded box for tfie ther-
mometers, which is now very widely used for temperature observa-
tions. The box is made of wood, and loovrod all round so as to
protect the thermometers inside from radiation, and at the same time
secure as free a circulation of air as is consistent with a satisfactory
protection from radiation. The box is painted white, both insid.^
and outside, and screwed to four stout wooden posts, also painter!
white, nrmly fixed in the ground. TIio posts are of such a length
that when the thennometcrs are hung in position the bulbs of the
minimum thermometer and hygrometer are exactly at the same
height of 4 feet above the ground, the maximum thermometer being
Fio. 1. — Thermometer
hung immediately above the minimum thermometer. Thij ther-
mometer box is placed over a plot of grass, and in a free ojien spies
to which the sunis rays have free access during as much of the day
as surrounding conditions admit of. It will be observed that tlie
thermometers ai-e suspended on cross-laths in the centre of the box
and face the door, which should always open to the north. It k
not possible to overestimate the importance of seeing thatuniformity
of height above ground and method of protecting the thermometers
is secured, since in no other way is it possible to obtain results from
different places which shall be comparable with each other and thus
supply satisfactory materials for the investi;^ation and development
of comparative climatology.
A desired uiuformity is yet far from being attained
among the meteorological systems of different countries.
Thus in Eussia the box for the protection of the thermo-
meters is made of zinc, on the supposition that such a box
follows more closely the changes of temperature of the air
than a box of wood. Owing to these international diversi-
ties of observation, it is extremely desirable that sfep.^
were taken to ascertain, by Joule's method of observing,
the approximate errors peculiar to each sort of thermometer
box, in order that the temperatures of different countries
may be compared together in a more satisfactory manner
than has yet been possible.
Interchanges of temperature among bodies take place by
conduction, convection, and radiation. In meteorology
the most important illustrations of conduction are the pro-
pagation do\™ wards through the earth's strata of the
changes of the temperature of the .surface as it is heated
dtiring the day and cooled diu-ing the night, and the pro-
pagation of the same changes of temperature through the
lowest stratum of the air which rests on the surface. Since
sand and light loose soils are much worse conduotors of
heat than clay and deuse soils, it follows that loose soils
116
METEOROLOGY
[didewl
and tracts of sand are subject during the. day to higher
temperature and during the night to lower temperature near
the surface than dense soils, and that frosts and extreme
temperatures do not penetrate so far into loose as into
dense soils.. It is on these differences that some of the
more striking features of climates depend. As snow is one
of the worst conductors of heat, owing to the quantity of air
tilling the interstices among the ice crystaU, it protects the
soil it covers by setting a limit to the dejjth to which the
(severe frosts of the surface penetrate, and by arresting the
escape of the heat of the soil ujjwards to the air.
The communication of heat from one part of the earth
to another by convection is seen on a grand scale in the
■winds and in the ciu-rents of the ocean. It is eeeu also in
the ascending and descending currents of the atmosphere
everywhere, which have their origin in the daily and
unequal changes of temperature to which the surface of the
eartJi is subject. The direct and beneficial effect which
results from atmospheric and oceanic circulation is a jnore
equable distribution of temperature over the globe, thus
moderating the rigours of the polar regions arid the heat
of the tropics.
An interchange of heat is constantly going on among
bodies exposed to each other, whatever be their tempcra-
tiu-e. This mode by which heat is communicated from
one body to another is called radiation. Radiant heat
proceeds in straight lines, diverging in all directions from
the source, is only in a limited degree influenced by the
air through which it passes, and is not diverted from the
straight course by the wind. The intensity is proportional
to the temperature of the source, and is greater according
to the degree of incUnation of the surface on which the
rays fall.
If then a body be placed in the presence of other bodies,
some colder and some warmer than itself, it will from this
mutual interchange of temj>erature receive more heat from
the warmer bodies than it radiates tb them, and conse-
quently becomes warmer ; but it will receive less heat from
the colder bodies than it radiates to . them, and its
temperature consequently falls. This is precisely the
condition in which the earth is placed in space. When a
part of the surface is turned towards the sun, that part of
the surface receives more heat than is radiated from it ;
and the temperature consequently rises most in that region
which for the time is perpendicular to the sun's rays, and
least round the annulus where the inclination of the surface
is greatest. On the other hand, since the hemisphere
turned from the sun radiates more heat than it receives
from the cold regions of space, the temperature there falls.
Owing to the essentially distinct conditions under which
the earth is placed with respect to radiation, the subject
falls naturally to be divided into two heads, solar radiation
and terrestrial radiation.
Solar Radiation. — Of the sun's rays which arrive at the
earth's surface, those which fall on tlie land and soUd
bodies generally are wholly absorbed by the thin surface
layer exposed to the heating rays, the temperature of
which consequently rises. Whilst the temperature of the
surface increases, a wave of heat is propagated downw:ards
through the soil. The intensity of the daily wave of
temperature rapidly lessens with the depth at a rate
depending on the conductivity of the soil, until at about 4
feet below the surface it ceases to be measurable. Part of
the heat of the surface layer is conveyed upwards through
the air by the convection currents which have their origin
in the heating of the lowennost stratum of air in direct
contact with the heated surface of the land.
Altogether different is the influence of the sun's rays on
■water. In this case the sun's heat is not all, indeed vej-y
l.\t from all, arrested at the sui face, but penetrates to a
considerable depth. The^ depth to which the influence of
the sun is felt has been shown by the observations made
during the cruise of the "Challenger" to be, roughly
speaking, about 500 feet below the surface of the sea.
The rate at which, in perfectly clear water, this heat \f,
distributed at different depths is a problem that has not
yet been worked out. Since water is a bad conductor, the
heat thus distributed does not, as takes place ■with resjiect
to land, penetrate to still lower depths by conduction, but
only ))y different densities prevailing at the same depth.?,
whether these different densities be due to different
temijcratures or different degrees of salinity. Thus one
of the more important distinctions between land and
water surfaces in their bearings on climate is that nearly
all the sun's heat falling on land is arrested on the surface,
whereas on water it is at once diffused downwards to a
great depth. In examining temperatures of the sea taken
at different depths, it is surprising to note the rapidity
with which changes of temperature are felt at considerable
depths, especially in cases when the temperature of the air
rises rapidly, accompanied wth strong sunshine.
In shallow water the sun's heat raises the temperature
much higher than that of deep water, this being obvious
from the consideration that nearly the whole of the sun's
heat which falls on the surface is utilized in raising the
temperature of the shallow layer of water ; in other
words, it is, so to speak, concentrated through a smal)
depth of water instead of being diffused through a gi-eat
depth.
Surface Temperature of the Sea. — The importance of a
knowledge of this datum of meteorology will be at once
recognized when it is kept in view that three-fourths of
the earth's surface is water, that the temperature of thi-
air resting on this surface is in close relation to the
temperature of the surface, and that the latter has, through
the intervention of the n-inds, direct and important
bearings on the temperature of the air over large portions
of the land surfaces of the globe. During the years
1859-63 Captain Thomas, while engaged on the survey of
the islands on the north-west of Scotland, made observa-
tions of the temperature of the surface of the sea every
hour of the day at all seasons, and with sufhcient
frequency for the determination of the diurnal range of
the temperature of the surface. The daily minimum,
0°"17 below the mean, occurred near 6 a.m.; the mean was
reached about 11 a.m., the maximum, 0°'13 above the
mean, between 3 and 4 p.m., and the mean again .shortly
before 2 a.m. Thus the dail}' oscillation of the temperature
of the surface of the sea amounted on the north-west of
Scotland only to 0°'3. In lower latitudes the amount of
the daily fluctuation is somewhat larger, but everj'where it
is comparatively small, if care be taken to make the
observations jiroperly, or at a distance from land, where
the influence of the heated or cooled land is not allowed
to vitiate the results.
Durmg the voyage of the "Challenger" a complete
system of meteorological observations, including the tem-
perature of the surface of the sea, was made every two
hours as part of the scientific work of the cruise. These
are now being discussed, and the writer of this article is,
by permission of the Lords Commissioners of H.if.
Treasury, allowed to use such of the results as have been
already arrived at.
The diurnal inarch of the teniperature of the surface of
the North Atlantic has boon determined from observations
made on one hundred and twenty-six days from ilarch to
August 1873 and in April and May 1876, the mean
latitude of all the ])oints of oKservation being nearly 30 N.,
and the longitude 42' W. The foUomng variations from
the mean .show the ])hases of this diurnal oscillation : —
TEMPERATHKE.]
2 a.m. -0-24
4 „ -0-33
6 „ -0-29
8 „ -012
METEOROLOGY
117
10 A.M.
Noon
2 P.M.
6 P.M. 0-26
8 „ 002
10 „ -019
Midnight -0-35
Thus in mid Atlantic, about 30° N. Up., where the sun's
heat is strong, and at the time of the year when the sun is
north of the equator, the diurnal fluctuation of the tempera-
ture of the surface is only 0°'80. It is highly probable
that nowhere over the ocean does the mean daily fluctuation
of the temperature of the surface quite amount to a degree.
This small daily fluctuation is a prime factor in meteorology,
particularly in discussions relating to atmospheric pressure
and winds.
Temperature of Air over the Open Sea. — The following
shows the daily march of the temperature of the air over
the North Atlantic on a mean of the same one hundred
and twenty-six days for which the temperature of the sea
has been given: —
1-13
10 A.M.
078
8 p.m. 0 73
1-40
Noon
1-45
8 „ -0-30
1-41
2 P.M.
1-80
10 „ -0-80
0 :!1
i »
1-58
Midnight -1 02
The amplitude of the daily fluctuation of the air is thus
3' 21, or nearly four times greater than that of the
sea over which it lies. Daring the same months the
" Challenger " was lying near land on seventy-sbc days.
The observations made on these days show a greater daily
range of temperature of the air than occurred out in the
open sea. The minimum, - 2°05, occurred at 4 A.M., and
the maximum, 2°33, at noon, thus giving a daily range of
4°'38. The occurrence of the maximum so early as noon is
doubtless occasioned by the greater strength of the sea
breeze after this hour, this maintaining a lower tempera-
tare. Part of the increased range of the temperature of
the air as compared with that of the sea was no doubt
due to the higher temperature during the day and the
lower during the night on the deck of the " Challenger " as
compared with that of the air. But, after making allow-
ance for this disturbing influence, it is certain that the
temperature of the air has a considerably larger daily range
than that of the sea on which it rests. The point is one
oi no small interest in atmospheric physics from the im-
portant bearings of the subject on the relations of the air
and its aqueous vapour to solar and terrestrial radiation.
The houily deviations from the mean daily temperature
of the air at two place.s, one near the equator and the other
in the north temperate zone, and both near the sea, viz.,
Eatavia (6° 8' S. lat., 10G° 48' E. long., mean temperature
78°'7) and Rothesay (55° 50' N. lat., 5° 4' W. long., mean
temjiorature 47°"3), are these : —
taUvla.
jlotIies.i>-.
Ikitttria.
Rothesay.
1 A.M. -3-2
-17
1 P.M. +57
+ 2*4
2 „ -3-6
-2-0 .
2 „ +5-6
+ 27
3 „ -40
-21
3 „ +5-2
+ 2-8
4 „ -4-3
-2-2
4 „ -I-4-3
+ 2-6
6 „ -47
-22
6 „ +3-3
+ 21
6 „ -4-9
6 „ +1-9
+ 1-5
' „ -4-3
-1-5
7 „ +0-6
+ 0-9
8 „ -2-2
-0-9
8 „ -0-4
+ 0-2
9 „ -Da
-0-2
9 „ -1-2
-0-4
10 „ +2-8
+ 0-5
10 „ -1-8
-=0-8
11 „ +4-4
+ 1-2
11 „ -2-3
-1-2
Koou +5 '4
+ 1-9
Midnight- 2-8
-1-5 1
The times of the four phases of the daily temperature at
Ratavia are — minimum about 5.50 A.M., mean 8.45 a.m.,
iiiaximnm 1.20 p.m., and mean 7.40 P.M. ; while for
Rothesay the .same times are 4.30 a.m., 9.15 a.m., 3 p.m.,
and 8.20 p.m. At Batavia, where the days and nights are
ntorly equal diuLng the year, there is little variation in
these times through the months ; but at Rothesay, where
the days are much longer in summer than in winter, there
is considerable variation in the tiines of occurrence of these
phases. The following table shows the times of the
phases for a number of selected places in the northern
hemisphere for the two extreme months, January and
July :—
January.
July. 1
Min.
Mean.
Mas.
ilean.
Mln.
Mean.
Mox.
Mean.
Sitka
6.0 '
6.20
6.50
6.0
5.30
7.20
6.50
6.0
4.30
5.30
6.50
7.10
6.30
6.0
5.40
9.40
10.0
10.0
10.40
10.10
10.10
10.5
10.0
8.25
9.25
9.60
9.50
9.35
9.10
S.O
I'.lo
1.60
2.40
1.30
2.30
2.0
2.40
2.0
0.55
1.30
2.35
2.25
2.30
2.10
0.40
6.36
9.40
8.45
9.0
8.0
7.0
8.35
8.0
6.46
8.15
7.45
7.50
8.20
8.5
6.45
3.*4b
3.50
5.0
2.40
3.30
3.40
4.40
3.15
3.0
3.40
4.30
6.0
5.30
5.30
5.0
7.40
8.15
8.40
8.36
9.0
8.45
8.50
8.15
8.10
7.35
8.20
9.5
8.45
9.0
8.45
O.M)
3.45
3.10
2.50
3.15
3.10
2.50
2.50
1.20
2.5
2.40
3.10
0.40
1.30
1.25
7.30
8.10
8.0
8.50
3.50
8.25
8.36
8.10
7.60
8.4
S.25
8.15
7. -30
6.30
8.60
Toronto
Philadelphia..
Havana
Archangel
Rothesay
Madrid
Geneva
.St Bernard.,..
Bogoslovsk....
Potroale.T;an- )
drovsk i
Tiflis
Calcutta
Bombay
During the night in summer the temperature falls con-
tinuously from the efiects of terrestrial radiation till the
earliest dawn, when the daily rise in the temperature sets
in ov.-ing to the heat reflected from the upper strata of the
atmosphere, which have begun to be heated and lighted
up by the rays of the morning sun. It will be observed
that the time of the daily minimum temperature occurs
earliest in high latitudes and latest in low latitudes.
During winter, on the other hand, the minimum tempera-
ture takes place in several regions some time before dawn.
At this season the two chief causes on which changes of
temperature depend are the sun and the passage of cyclones
and anticyclones ; and it is probable that those cases whera
the minimum occurs markedly before the dawn are, where
not occasioned by purely local disturbing causes, due to
the mean diurnal times of occurrence of the changes of
temperature which accompany the great atmospheric dis-
turbances of cyclones and anticyclones.
In July the daily maximum temperature occurs generally
from 2 to 4 p.m. At places, however, near the sea, which
are within the immediate influence of the sea breeze, and
in places at 'some distance from the sea, such as Calcutta,
where the wind, being essentially a sea wind, attains its
greatest .daily velocity and the sky at the same time is
much clouded, the maxinjum occurs nearly two hours
earlier. In high situations, such as the St Bernard hospice,
the highest daUy temperature also occurs nearly two hours
sooner than on the plains below. In the ■R'iuter months
the maximum is about an hour earlier than in the
summer.
In investigating 'Ae daily curves of temperature. Sir
David Brewster drew several interesting conclusions from
them. By dividing the daily curve of temperature, deduced
from the mean of the year, into four portions, at the points
representing the two daily means and the two extremes,
he showed that the four portions approximate to parabolas,
in which the temperatures are the abscissae and the hours
the ordinates. The correspondence between the observed
and calculated results is so close that the difference did
not in any case exceed a quarter of a degree Fahrenheit
This interesting result is true for places at which the
horizon is open all round, so that no shadows of hills,
trees, or buildings fall on the places where the therpio-
meters are kept during the day. If a hill rises to ibc
118
METEOROLOGY
[TEMrErATUiir.
north of the place, by which the sun's rays are never
obstructeU, it exercises little, if any, influence on the
observations ; but if one or more hills obstruct the rays
of the sun after it has risen above the horizon, such obstruc-
tion affects the temperature while, and for some time
after, the position in which the thermometer is placed is
shaded from the sun.
Brewster further made the important remark that tne
mean of observations made at any pair of hours of the
same name, such as 8 a.m. and 8 p.m., 9 a.m. and 9 p.m.,
&c., does not differ much from the mean temperature of
the day. The pairs of hours which approximate closest to
the true daily mean are 9 a.m. and 9 p.m., 10 a.m. and 10
P.M., 3 a.m. and 3 p.m., and i a.m. and 4 pm. The mean
of four hours at equal intervals from each other gives a
result still closer to the true mean temperature.
Ill organiziug any system of meteorological observptioh, by which
it is intended to develop the climatology of the country, the de-
termination of the hours of observation is a question of the first
importance. If only two observations be made daily the best houi-s
are 9 A.M. and 9 p.m., or 10 a.m. and 10 p.m. ; and if there be four
observations the best hours are 3 and 9 A.M. and 3 and 9 p.m.,
or i and 10 a.m. and 4 and 10 p.M- If there be three observa-
tions the best hours are 9 A.M. and 3 and 9 p..m. , or 10 .\.M.
and 4 and 10 p.m.; but in these cases it is essential that the
observations of a minimum tliermoraoter be added to the tempera-
ture observations. Theso liours are further strongly recommended
by the consideration that they are approximately coincident with
the diurnal phases of atmospheric pressure, an exact knowledge
of which lies at the root of nearly all cUmatological inquiries.
The three equidistant hours which have been adopted in several
countries, viz., 6 a.m. and 2 and 10 P.M., are only good as regards
the temperature, not as regards atmospheric ))ressnre. With re-
spect to two daily observations, the liours S a.m. and 1 p.m., which
have been adopted in some countries, are singularly unsuitable
for the furnishing of the observational data required in the de-
velopment of the climatologies of these countries; and, what is
still more serious in a science where international co-operation is so
imperatively demanded, these observations cannot be used with
any satisfaction in such deeply important inquiries as the com-
parative climatologies of Europe.
The times of occurrence of the highest, lowest, and
mean daily temperatures, and the amount of the daily
range of temperature, are in a great degree influenced by
the covering or want of covering of the earth's siu'face on
which the air rests. ^Vhen the ground is covered with
Tegetation, the whole of the solar heat falls on the
vegetable covering ; and, as none falls immediately on the
Boil, its temperature does not rise so high as happens where
there is no vegetable covering to shade Uie surface from
the sun. The temperature of plants exposed to the sun is
not so high as tiat of exjiosed soil in the vicinity. As
regards forest.s, the four diurnal pha,ses of temperature
occur later than in the open countr|-, and the ina.xiinuni
and minimum are less decided ; and, since the maximum
temperature of the air in forests falls short of the maximum
in the open to a considerably greater extent than the
minimum under trees is above the minimum in the open,
it follows that the mean temperature of the air in forests
is le.ss than that of the open country adjoining. The
reason of the .difference is that the chilling effects of
nocturnal radiation penetrate lov/er down among' the trees
than do the heating effects of .solar radiation ; and as the
soil is not heated directly by the sun its temperature is
lower, and consequently that of the air over it is also
lower. A cleared space in a forest, sheltered by the sur-
rounding trees, but ojien to the sun, has a warmer and
moister atmosphere in spring and summer and very much
moister in autumn than prevails in the open country
adjoining, and has also the diurnal differences of range
pectiliar to a warmer and moister atmosphere.
One of the most important elements of climate is dis-
rlo.sed by the difference between the hour of lowest and
the hour of highest mean temperature respectively, or, as
it is usually exjiressed, by the daily range of temperature.
We have seen that as regards the sea in the north-west nf
Scotland the difference is only 0°'3 and in the Atlantic
about 30^ N. lat. 0''8, and that probably the diurnal range
of temperature of the surface of the sea nowhere amounts to
a degree. In the .same part of the Atlantic the daily range
of the temperature of the air resting on the ocean is 3°'2,
and on the .sea near land 4'-4. On advancing on the land,
the daily range of temperature rapidly increases, and the
rate of increase is greatly augmented when an inland
position is arrived at to which any sea breezes that may
prevail do not extend.
The true daily range of temperature is stated by ob.ser-
vations made with maximum and minimum thermometers.
Generally speaking, the amount of the range increases as
the latitude is dinxinished, and as the distance from the sea
is increased, but above all it increases in proportion to the
dryness of the climate.
The dilFerences of this vital element of climate pvcstrikmgly.showu
in the meteorology of India. In the Jleimrt for 1S80 the following
ai-e tile mean daily ranges of March of that year at a few places :
at Goa 5°'4, Bombay 11 '2, Kurrachce 23^*5, Jacobubad 37*'4, and
Pachbudra (lat. 25° 55' N., long. 72° IS' E.) 41°-3. In the last
case, midoubtedly one of the greatest mean daily ranges of tem-
perature meteorology has yet recorded, the mean of tlic days was
103°-4 and of the nights 02°1. As .March is altogether within
the season of the north-east monsoon, the general drift of the
wind over western India, where these are situated, is fi-om the
interior towards the sea, subject as I'egards Bombay and Goa I*
the influences of the land and the sea breeze. On the other hand,
in June, when the south-west monsoon has fairly .set in, tliJ
following are the mean daily raugfs of temperature at the s.inie
places; at Goa 5"-6, Bomb.iy 8°-2, Kurrachee 10°, Jacokibad 27°'fi,
and ?.ichbudra 24°'l. These show in a striking manner the
powerful influence of the moister atmosphere spread over India by
the south-west monsoon, under which tlic daily range of tenipera-
turc falls at Kurrachee from 2.'j° 5 to 10°, and in the cxcewivcly
arid climate of Pachbudra from 41°-3 to 24°'l. In these Jry
climatcs of the Imsin of the Indus, whilst the rainfall both in Jlarch
and in Juno is practically nil, yet the relative huniidity of '.hf.
atmosphere is widely JifTeront. 'i'hus the humidities for ilai-ch and
Juno respectively at 4 P.M., wiien the temperature is nearly the
maximum for the day, are 43 and 77 for Kurrachce, IS and 30 for
Jacobabad, and 11 and 36 for Pachbudra. It is not so much the
amount of cloud that determines the degree of fierceness of the sun's
heat in these climates as the relative humidity, or the dryness of
the air, as pointed out by Strachey in 1866. Thus at Jacobabad
less than half tlie amount of cloud appears in the sky in June
as compared with March, but the relative humidities are 30
and 18, and the daily range of temperature 27''-6 and 37°-4. If
we except the dry arid wastes of I ei-sia and Arabia, there i.^
perhaps no other region of the globe where the daily lange of
temperature approaches that of the valley of the Indus. Thui
in tlie dry climates of such places as baci-amento (California)
in summer it amounts only to about 30°, at Madrid to 27°, anJ
JeriLsalcm 24°. In central districts in the south of Rn;^land
it is about 20°; farther north it falls to 15°; and in the islands
in the north, whose climate is strictly insular in its character,
the summer daily range is only 10°. Ill Arctic regions, sucli
as Spitsbergen and Boothia Felix, the range in .winter varies
from 0"'0 to l^'O; in May, when the sun has reappeared and
continues to rise and set, it rises to 14°; but iu July, when the
sun docs not set, tlie range sinks to 10°.
But maximum and minimum thermometers not only
show the mean daily range of temperature, they are also
of great utility in giving observations for the determination
of mean temperatvire. The mean temperature may bj
accepted ;'.s the mean of the twenty-four hourly ob.serva-
tions of the day. If with such a system of observation
daily readings of the maximum and minimum thermometer
be compared, the value of the latter observations in
questions of mean temiterature may be arrived at. Double
.series of observations of this description have been made
at mauj' ])laces. The following shows a comparison of the
mean of maximum and minimum daily temperatures with
means from observations made twenty-four times daily,
the former exceeding the latter means in nearly iH
cases : —
METEOROLOGY
Biitavia
Calcutta
Peking 0
Nertcliiiisk | 0
B.irnnul
Ekntermbu'.g....
Tiflis
St Petersburg....
Yalcntia
Grefnwich
Rothesay
>,.:..,.
Sninmer.
^jituiiin.
Wli.rtv,
Year, i
-OS
-0-2
-0 2
-0-2
-0-2
vo
0-7
0-7
0 9
0-8
0-6
0-6
0-6
0-7
0-6
Oi
0-8
€■6
10
0-3
0-5
Of)
0-7
0-8
0-6
ori
0-7
Of
0-6
0 0
0-5
0-5
0-5
0-4
0-6
0-6
0-6
0-3
0 1
0-4
0-4
0-5
0-1
-0-1
0-2
07
0-8
0-6
0-0
0-4
0-4
0-3
0-3
0-3
0-3
These results show remarkable uniformity, and it may
he inferred from them that mean temperatures deduced
from maximum and minimum observations are about half
a degree above the true mean temperature. Ip general
climatological inquiries, obs\rvations with these thermo-
meters have the strong recommendation of supplj-ing from
observations taken once a day the data for the determina-
tion of the mean temperature and mean daily range of
localities ; to which falls to be added the further advantage
of giving results more uniformly comparable for different
places than could be afforded by observations made with a
common thermometer at any single hour or pair of hours
daily.
Daily Variation of the Humidity of the Air. — The
gaseous envelope surrounding the earth is composed of
two atmospheres, quite distinct from each other, — an
atmosphere of dry air and an atmosphere of aqueous
vapour. The dry air, which consists of oxygen and
nitrogen, is always a gas, and its quantity remains constant ;
but the aqueous vapour doe-s not continue permanently in
the gaseous state, and the quantity present in the air is,
by the ceaseless processes of evaporation and condensation,
constantly changing. If the aqueous -.vapour remained
permanently and unchanged in the atmosphere, or were
not liable to be condensed into cloud or rain, the mixtiure
would become as complete as that of the oxygen and
nitrogen of the air. The equilibrium of the vapour atmo-
Ephere, however, is being constantly disturbed by every
change of temperature, by every instance of condensation,
and by the unceasing process of evaporation. Since dry
air further materially obstructs the free diffusion of the
aqueous vapour, it follows that the law of the independent
pressure of the vapour and of the dry air of the atmosphere
holds good only approximately. The aqueous vapoiu-,
however, constantly tends to approach this state. Since,
then, the independent and equal diffusion of the dry air
and the aqueous vapour is, owing to these disturbing causes,
never reached, the important conclusion follows that the
hygrometer can never indicate more than the local humidity
of the place where it is observed. Hygrometric observa-
tions can therefore be regarded only as approximations to
a true indication of the quantity of aqueous vapotir in the
atmosphere over the place of observation. It is, however,
to be added that, while in certain cases the amount of vapour
indicated is far from the truth, yet in averages, particularly
long averages, a close approximation to the real amount is
reached it the hygrometer be at all tolerably well exposed
and carefuUy observed.
Aqueous vapour is constantly being added to the air
from the surfaces of water, snow, and ice, from moist
Burfaces, and from plants. The rate of evaporation
increases with an increase of temperature, because the
capacity of the air for vapour is thereby increased. The
atmosphere can contain only a certain definite amount of
vapour, according to the temperature ; when therefore the
air has its full complement of vapovur, or when, in other
'■words, it is saturated, evaporation ceases. Thus the rate
of evaporation is greatest when the air is driest or frctot
119
from vapour, and Iea?t when the air is nearest the point of
•saturation. Since currents of air remove the moister and
substitute drier air over the evaporating surfaces, evapora-
tion is much more rapid during wind than in calm weather.
As air expands under a diminished pressure, its temperature
consequently falls, and it continues to approach nearer to
the point of satm-ation, or become moister ; and, as it
contracts under an increased pressure, its temperature rises
and it recedes from the point of saturation or becomes
drier. Hence ascending currents of air become moister
■with every addition to the ascent, and descending currents
drier as they continue to descend. Thus as muds ascend
the slopes of hills they become moister, but Miien they
have crossed the summit and flow down the other side
they become drier in proportion to the descent, and all the
changes ma)' be experienced from extreme dryness to
saturation in the same mass of air, which all the time has
practically had its amount of aqueous vapour neither added
to nor diminished.
In an atmosphere Oi air and aqueous vajwur perfectly
mixed, the elastic force of each at the surface of the earth
is the pressure of each. In this case the elastic force of
aqueous vapour would be the pressure of the whole vapour
in the atmosphere over the place of observation. This
pressure is expressed in inches of mercury of the barometer.
If we suppose the total barometric [jrcssure to be 30 '000
inches, and the elastic force of vapour to be 0'7.4.t inch,
the presstire or weight of the dry air, or air proper, would
be 29'25.5 inches, and of the aqueous vapour 0'745 inch.
From this it follows that the elastic force of vapotu- may
be regarded as indicating the quantity of aqueous vapour
in the air at the place of observation, or it may be desig-
nated the absolute humidity of the air.
The diurnal variation in the elastic force of vapour in
the air is seen in its simplest form on the open sea.
Grouping together all the hygrometric observations made
ou board the "Challenger" on the North Atlantic at a
distance from land, from March to July 1873 (eighty-four
days), we have for that time a mean elastic force of 0'6.59
inch, and the following diurnal variation : —
Inch.
1 Inch.
Inch.
2 a.m. --015
10AM. + -004
6 r. M. + -007
4 „ --020
Noou +-017
8 „ +-002
6 „ - -016
2 I'.M. -1- -020
10 „ --005
8 „ --007
4 „. -^■0l7
Midnight +003
Hence the minimum ( - '020 inch) occurs at the hoiu-
when the temperature of the surface of the sea and air
resting over it falls to the daily minimum ; it then rises
to the mean a little after 9 a.m.. and to the daily maximum
( + '020 inch) at 2 p.m., when the sea and air are abo near
the daily maximimi, and falls to the mean shortly before
9 P.M.
Treating the observations made near land by the
"Challenger" during the same months, the following is
the diurnal variation disclosed : —
Inch.
Inch.
iDCJl.
2 a.m. - -003
10 A.M. + -014
6 P.M. -000
4 „ --009
Noou -1- ■oil
8 ,, --004
6 „ - -010
2 P.M. -1- -007
10 „ --005
8 „ - -003
4 „ -h'015
Midnight -007
The disturbance induced by proximity to land in the
distribution of the aqueous vapour in the lower strata of
the atmosphere is very strijdng. The maximum and
minimum no longer follow the corresponding phases of the
temperature of the surface of the sea and of the air. Tlie
disturbing agents are the sea and land breezes and their
effects. Under the influence of the land breeze the time
of the minimum humidity is delayed till about 6 a.m.; and
under the influence of the sea breeze and its effects the
amount of the aqueous vapour shov.-s a secondary minimum
from noon to 2 P.M. It is to be here noted that this midday
120
METEOKOLOGY
[dew.
niimmum occm-,- at the hours ol' the day when the sui-face
of the land i< most higlily heated, the ascending current
<il' heated air ri^iny from it therefore strongest, and the
ri;suJtinK breeze from the sen towards the land also strongest.
Xow it dots not admit of a doubt that the diminution in
the amount of the aqueous vapour noted on Vioard the
"Challenger'' near the shore points to an intermLxture
with the air forming the sea breeze of descending thin
air-filanients or currents to supply the place of the masses
of air removed by the ascending currents which rise from
the heated surface of the land. At Batavia, on the north
coast of Java, and at Bombay, the aqueous vapour is also
subject to a secondary minimum during the warmest hours
of the day.
During the summer months this secondary minimum is
best iuarked at inland places such as Peking, Nertcliinsk,
Barnaul, Tiflis, and Ekaterinburg, but the time of its
occurrence is about two hours later than it is over the
Xorth Atlantic. Over all these places at this season the
ascending current from the heated land in the interior of
Asia is very strong. On the other hand the lowering of
the amount of aqueous vajjoiir scarcely if at all appiears as
a feature in the summer climate of St Petersburg, and
not at all in that of Sitka, where the sea breeze is equally
not a constant feature of the clirjate of the district.
In the e.\co3sivi-ly dry, rainless, and hot climate of Allahabad, in
April tliL- iliurnal minimum of the ariueous vapour occui-s from
11 A.M. to 6 P.M., the time of absolute minimum being 2 and
3 P.M. During all otlicr hours of the day the amount of the
vapour Id above the mean, a secondary minimum occurring from
1 to 1 .\.M. At Allahabad, at this time, the absolute m.axi-
mum vapour pressure occ "s at 8 A.M. Quit* similar to this is
the dlurual distrilnition of ilic aqueous vapour in July at Lisbon
and Coimbri, the minimum occuriing from 10 .\. M. to 3 P.M. At
this time of the year the climate of this part of the peninsula is
hot aud dry and the rainl'all insignificant in amount. As this
region lies between the liigh atmosjdieric pressure so characteristic
a feature of the meteorology of the Atlantic in summer and the
comparatively low pressure over the continents southward and
eastward, the winds are almost wholly north-westerly. In this
connexion it is instructive to note that the time of maximum
vapour pressure is from 4 to 7 A.M., when the velocity of the wind
is near the minimum, and the chief minimum vapour pressure
from noon to 4 P.M., when the velocity of the wind and ascend-
ing current.= roach the daily maximum. These results show that
the diminution iu the vapour pressure during the houi-s wdieu
temperature is highest, which chaiucterizes the cUmates of large
tracts of the globe, is due to descending air-filaments or currents,
wliich necessarily accompany the ascending currents that rise from
the heated land.
At Geneva during liie summer months the vapour curve exhibits
two daily minima very strongly marked, the one shortly before
Hunrise aud the other from 2 to 4 P.M., and two maxima, one
from 8 to 11 A..M. and the other from o' to 10 p.m.; and with
these the thurnal variations of cloud are in accordance. The
peculiarly marked features of the vapom- cm-ve at Geneva az'e
probably duo to the size of the lake, which is large enough to
gi\o rise to a decided breeze during the day from the lake all
round its shores and during the night to a breeze from the land
all round u[>ou the lake. On the setting ia of the breeze, the
mass of air composing it, having been for seme time resting on
the lake, is rather moist, an-l cnus one of the daily maxima is
brouglit about from 8 to 11 a.m. As the breeze continues the air
supplying it is necessarily drawn from the higher strata of the
atmosphere more copiously than in different situations ; and, having
tiius acquired increased dryness in the descent, and having blowu
over the lake for too short a distance to mateiially influence its '
moisture, the air becomes constantly drier, till the minimum
from 2 to 4 P.M. is reached. The lake breeze thereafter begins to
diminish in force, and the air consequently becomes moistertill the
maximum vapour pressure of the day occurs wiien the lake breeze
dies away and the land breeze has not yet sprang up. In the
winter months, when these breezes do not prevail, the curve of
diurnal vapour pressure shows only one maximum and minimum.
TLe reliitive humiditi/ of the atmosplicre must not be
confounded with its vapour pressure or absolute humidity.
The relative humidity, or, as it is more frequently <;allcd,
the humidity, of the air is the degree of its approach to
saturation. Complete saturation is represented by 100
and air absolutely free of vapour by 0, the ktter state of
things never occurring in the atmosphere, a htmiidity of
10 being of rare occurrence even in such arid regions as
those of Arabia. The great significance of this element of
climate is in its relations to the diathermancy of the air,
and consequently to solar aud terrestrial radiation. It is
supposed that perfectly dry air would allow rays of heat
to pass through it with at most only a very slight
increase to its temperature therefrom. Let, however, a
little aqueous vapour be added to it, a partial obstruction
to the passage of radiant heat is offered, and the temjjera-
ture of. the mixture, or common air, is sensibly raised.
Hence, other things being equal, the less the amount of
vapour the more are the effects of radiation felt, or the
greater the heat of the days and the cold of the nights.
The mere amount of vapour in the air does not determine
the degree of radiation, but it is the amoimt of vaix)ur
together with a certain temperature — in other words, the
absolute and relative humidity of the air taken together —
that determines the heating power of the sun and the
degree of cold produced by terrestrial radiation.
The diurnal variation of the relative hiimidity is very
different from that of the vapour pressure, and presents
features of the simplest character. Tlie following are the
diurnal variations from the mean humidity 80 over the
North Atlantic, from the "Challenger" observations in
1873 •—
■2A.yi.+2
6 P.M.
10 A.M. -1
oon - i
P.M. - ;
Midnight -(-2
Thus the maximum humidity occurs from midnight to
4 A.M., or when the d&ily temperature is at the minimum,
and the minimum humidity at 2 p.m., when the tempera-
ture is at the maximum, the curve of humidity being thus
inverse to that of the temperature. With two slight
modifications this is the diurnal humidity curve for all
climates and seasons. In the calm which intervenes in
the morning between the land and the sea breeze the
humidity continues high, or even increases, though at the
time the diurnal -increase of temperature has already set
in. The other modification is seen in the humidity ciurves
for Nertchinsk and Barnaul during winter, these curves
being not inverse but coincident with the daily curves of
temi)erature. In the climates of Central Asia in winter,
the amount of vapour is very small, and the increase to
the relative humidity during the day is probably occasioned
by the more active evaporation from the snow during the
day and the stillness of the air favouring the accumidation
of aqueous vapour near the surface of the earth.
Next to the winds, the aqueous vapour of the atmo-
sphere, in the diverse ways in which in different localities
it is distributed through the hours of the day, plays the
most important part in giving to the ditferent parts of the
globe its infinitely diversified climates.
Detv.- — Dew is deposited over the earth's surface on
comparatively clear aud calm nights. As the cooling by
terrestrial radiation continues, the temperatiu-e of objects
on the surface is gradually lowered to the dew-point, and
wheu this point is reached the aqueous vapour begins to
be condensed into dew on their surfaces. The quantity
deposited is in proportion to the degree of cold produced
and the quantity of vapour in the air. Dew is not
deposited in cloudy weather, because clouds obstruct the
escape of heat by radiation, nor in windy weather,
because wind continually renews the air in contact with
the surface, thus preventing the temperature from falling
sufficiently low. Vljen the temperature is below 32°, dew
freezes as it is deposited, and hoar-frost is produced. The
dew-point practically determines the minimum teniperatiue
BAEOKCETRIC OSCILLATIONS.] METEOROLOGY
of the night, — because if the temperature falls a little
below the dew-point the liberation of heat as the vapour
is condensed into dew speedily raises it, and if it rises
higher the loss of heat by radiation speedily lowers it.
This consideration suggests an important practical use of
the hygrometer, it being evident that by ascertaining the
dew-point the approach of frost or low temperature likely
to injure vegetation may be foreseen and provided against.
Diurnal Oscillations of ihe Barometer. — The general
character of the daUy oscillations of atmospheric pressure
is shown by the two curves of fig. 2. The solid
line gives the mean oscillation for Bombay and tie
-m
\i \\/-
O ' 1 ' 1
-m"n-
"T
\
\
\
.
'
*.. \
/
\,
'*•.
"A
/ '
\ ■■
V.
A-
\
\ '" ,
7
■N.
\
■/
x
/
^
. 1 1
Mill
,1 1 1 1.1-
J_J_J_LJ.
1
Fig. 2. — Daily Oscillations of Atmospheric Pressure.
dotted line that for Vienna, these two curves being to
a large extent tyjncal of diurnal barometric oscillations in
tropical and temperate regions as regards the two maxima
and minima and the time of their occurrence.
A series of twelve maps of the globe were prepared for
June, showing, for all stations whence observations have
been obtained, the deviations at noon, 2 p.m., 4 p.m.,
4c., Greenwich mean time, from the mean daily pressure ;
and four lines were drawn indicating the positions of the
two daily maxima and minima at these hours. For fully
30° north and south of the equator the lines of maxima
and minima run north and south, but in higher latitudes
these directions are changed, and the changes are chiefly
conspicuous as regards the A.M. maximum and the p.m.
minimum. Thus, for example, at 6 p.m. (Q. M. T.) the
line of P.M. Tnininiiim is for the latitude of London near
16* W. long. ; in 30° N. lat. it is in 35° W. long., in which
the line runs south as far as 30° S. lat. ; its course thence
turns south-westwards to near the Falkland Islands, 60°
W. long. Hence in June the p.m. minimum occurs about
three hours earlier in the Falkland Islands than to the
south-west of Ireland, thus showing in a striking manner
the influence of season on this phenomenon. In the middle
and higher latitudes in summer, proximity to the sea
delays the time of occurrence of the a.m. maximtim and
the p.m. minimum ; whilst in continental situations the
A.M. maximum occurs much earlier than in lower latitudes,
and the p.m. minimum nearly as late as at places near the
sea. In cases where the lines of maxima and minima
cross a region such as southern and western Europe, whose
surface is diversified by large tracts of land and sheets of
water, the deflexions are of a remarkable character.
The retardation of the time of occurrence of the A.M.
maximum is greatest in situations which, while eminently
insular in character, are at the same time not far from an
extensive tract of land. Of this Holland presents the best
example in Europe ; and there the a.m. maximum, which
at Paris occurs at 8 a.m., does not occur at Utrecht tUl
9.30 A.M., at Amsterdam till 12.30 p.m., and at Helder till
2 p.m. There is thus as regards the same diurnal pheno-
menon in June a difference of six hours between Paris and
Helder. Sicily and the south of Italy on the one hand
and Madrid on the other present also the most striking
contrasts. Again at Sitka (56° 50' K lat., 135° W. long.),
. which has one of the most truly insular climates in the
world, the a.m. maximum is delayed to 2.30 p.m. ; whereas
Hi— ?•
121
at Astoria, ten degrees to southward, it occurs at 9.30
A.M., _and at Fort Clnuvliill, in Nevada, as early as
7 A.M. There is thus as regards the, same phenomenon
a difference of 1'^ 30" between Sitka and Fort Churchill.
From hourly observations made in this month at the
base, the top, and two intermediate points on Mount
T7ashington (N. H.) it was found that the time of occur-
rence of the A.M. maximum at the base of the mountain,
which is 2898 feet above the sea, was S A.st. ; at 4059
feet, 10 A.M. ; at 5533 feet, 11 a.m.; and at the top,
6285 feet, noon. Hence, as regards the time of occur-
rence, the influence of an isolated mountain like Mount
Washington brings about a result similar to what is
observed in insular situations. But the analogy is even
closer. In insular climates the minimum in the early
morrung is very greatly in excess of that in the afternoon ;
and the same relation is observed on the top of Mount
ATashington, where the former is - 0'020 inch and the
latter - 0'004 inch. Again in continental climates the
minimum in the early morning is much the smaller of the
two, and the same relation -was observed at the base of the
mountain, where the observed minima were respectively
0'006 inch and 0020 inch. The differences presented by
the daily curve of pressure at the top as compared ^vith
that at the base of the mountain have their explanation in
the effects which follow the diurnal range of temperature.
As the temperature Ls at the minimum at the time of least
pressure in the morning, the atmosphere is more condensed
in the stratum between the base and the top, and conse-
quently the barometer at the top reads relatively lower.
hs the temperature continues to rise during the day, the
stratum of air above the base of the mountain expands,
thus placing more air above the barometer at the top, so
that, while at the base pressure begins to fall at 8 a.m.,
at the top it continues to rise till noon, simply from the
mechanical upheaval of the air owing to the higher tempera-
ture. In the afternoon, when the minimum at the ba.se
falls to - 0'020 inch, it is only - 0-004 inch at the top, this
relatively higher pressure at the top being due to expansion
from temperature. The peculiar feature of the pressure
curve at the top is essentially a temperature effect.
The diurnal oscillations of the barometer occur alike
over the open sea and over the land surfaces of the
globe. The atmosphere over the open sea, as already
shown, rests on a floor or surface subject to a diurnal
range of temperature so small as to render that temperature
practically a constant both day and night. This considera-
tion leads to the vital and all-important conclusion that the
diurnal oscillations of the barometer are not caused by the
heating and cooling of the earth's surface by solar and
terrestrial radiation and by the effects which follow these
diurnal changes in the temperature of the surface, but that
they are primarily caused by the direct and immediate
heating by solar radiation, and cooling by nocturnal radif.-
tion to the cold regions of space, of the molecules of the
air, and of its aqueous vapour. These changes of tem-
perature are instantly communicated through the whole
atmosphere from its lowermost stratum resting on the
earth's surface to the extreme limit of the atmosphere,
which the flight of meteors proves to be not less than 500
miles There are important modifications affecting the
amplitude and times of occurrence of the four prominent
phases of the phenomena observed over land surfaces, the
temperature of which is being superheated during the day
and cooled during the night ; but it is particularly to be
noted that the barometric oscillations themselves are inde-
pendent of any changes of temperature of the floor on
which thfe atmosphere rests.
Let us first look at the phenomena iu the simplest form
as found in the Pacific, or in the midst of the largest water
22
M ±: T E 0 R 0 L 0 G T
[baromktbio
.ariace of the gloVio. The following are the mean varia-
tions of pressure from observation:! made on board the
"Challenger," September 1 to 12, 1875, in mean latitude
r 8' S. and long. 150° -iO' "W, the mean being 29-938
inches : —
A. M. -0012
10 A.M
0-032
6 P.M. -0-023
„ -0022
Noon
0-006
8 „ 0-004
0-003
2 P.M.
-0-043
10 „ 0-013
0028
i »
-0-055
Mianight 0-012
The nio.st striking feature in these oscillations is the
amplitude of the range from the a.m. maximum to the
P.M. minimum, amounting to 0-087 inch, and the rapidity
of the fall from 10 A.M. to 2 p.m. The same feature
appears in all means deduced from observations made at
least 12* on each side of the equator.
, From October 12 to 22, 1875, in mean lat. 35° 1' S., long.
134° 35' W., the mean atmospheric pressure was 30-298
inches, and the difference bet-sveen the a.m. maximum and
the p.m. minimum -n-as only 0-036 inch ; and from July 12
to 19, 1875, in mean lat. 36° 16' N. and long. 156°
ir W., the mean pressure -was 30'328 inches, and the
difference between the a.m. maximum and p.m. minimum
Was only 0-025 inch. Thus, with a mean pressure in the
Pacific about lat. 35°-36° N. and S. much greater than
near the equator, the oscillation is much less, being in the
North Pacific less than a third of what occurs near the
equator. Similarly, this oscillation is small (or even smaller)
in the high-pressure areas in the North and South Atlantic
as compared wth the same oscillation near the equator.
It is well known that aqueous vapour absorbs the heat
rays of the sun considerably more than does the dry air of
the atmosphere ; how much more physicists have not yet
accurately determined. Consequently air heavily charged
with aqueous vapour will be heated directly by the sun's
rays as they pass through it in a greater degree than
comparatively dry air is. Now it is shown further on that
the prevailing surface -winds outflow in every direction
from the areas of high mean pressure in the Atlantic and
Pacific about lat. 36° N. and S. Since, notwithstanding,
the pressure continues high, it necessarily follows that the
high pressure is maintained by an inflow of upper ciu-rents,
and as the slow descending movement of the air connects
the inflowing upper currents with the outflowing prevailing
winds of the surface, it follows that the air over high-
pre6.sure areas is very dry, and that it is driest where
jiressui-e is highest and the high-pressure area best defined.
-Hence over the best-defined auticyclonic regions the air wJl
be least raised in temperature through all its height by
the heat rays of the sun.
On the other hand, between these high-pressure areas of
great oceans there is a belt of comparatively low pressure
towards which the north and south trades pour their
vapour unceasingly. The atmosphere of this belt of low
pressure is thus highly saturated with aqueous vapour
which rises in a vast ascending stream of moist air to the
higher regions of the atmosphere. These equatorial regions
thus present to the sun a highly saturated atmosphere
reaching to a very great height. It is in these regions
therefore t!i3t the atmosphere will be most highly heated
by the sun's heat rays as they pass through it. One of
the most striking facts of meteorology is the suddenness
with which this barometric oscillation increases in amplitude
on entering on these parts of intertropical regions ; and
the rapidity with which its amplitude diminishes on
idvancing on the high-pressure regions of the horse
latitudes is equally striking. The following are the mean
oscillations in the middle regions of the funr great oceans
about lat. 36° from the a.m. maximum to the v.yi. minimum
about the time of the year in each ease when the sun
is highest in the heavens : — South Pacific. O'OSG inch ;
North Pacific, 0-026 indi; g«Utli Atlantic, 0-024 inch;
and North Atlantic, 0-014 inch. These amplittidea
diminish as the oi-ean becomes more land-locked with
continents, or as the auticyclonic region becomes better
defined and currents of air are poured down more steadily
from the higher region.} of the atmosphere.
If the temperature of the whole of the earth's atmosphori
were raised, atmospheric pressure would be diminished,
for the simple reason that the mass of the atmospherM
would thereby be removed to a greater distance from th^j
earth's centre of gravity. Quite different result.?, however,
would follow if the temperature of orJy a section of the
earth's atmosphere were simultaneously raised, such a.^ the
section comprised bet%veen long. 20° and 60° W. The
immediate effect would be an increase of barometric
pressure, o\\-ing to expansion from the higher temperature ;
and a subsequent effect would be the setting in of an
ascending current more or less powerful, according to the
differences between the temperature of the heated section
and that of the air on each side. These are essentially
the conditions under which the morning maximum a'^''
afternoon minimum of atmospheric pressure take place.
The earth makes a complete revolution round its axi3
in twenty-four hours, and in the same brief interval the
double-crested and double-troughed atmospheric diurna'.
tide makes a complete circuit of the globe. The whole of
the diurnal phenomenon of the atmospheric tides is there-
fore rapidly propagated over the surface of the earth from
east to west, the movement being most rapid in equatorial
regions, and there the amplitude of the oscillations ia
greater than in higher latitudes under similar atmospheric,
astronomical, and geographical conditions. Owing to the
rapidity of the diurnal heating of the atmosphere by the
sun through its whole height, some time elapses before the
higher expansive force called into play by the increase of
temperature can counteract the vertical and lateral resist-
ance it meets from the inertia and viscosity of the air.
Till this resistance is overcome, the barometer continues
to rise, not because the mass of atmosphere overhead is
increased, but because a higher temperature has increased
the tension or pressure. 'When the resistance has been
overcome, an ascending current of the -B'arra air sets in, the
tension begins to be reduced, and the barometer falls and
continues to fall till the afternoon minimum is reached.
Thus the forenoon maximum and afternoon minimum are
simply a temperature effect, the amplitude of the oscillation
being determined by latitude, the quantity of aqueous
vapour overhead, and the sun's place in the sky.
Vll observations show that over the ocean, latitude for
latitude, the amplitude of the oscillations is greater in an
atmosphere highly charged with aqueous vapour and less
in a dry atmosphere. It is also to be noted that in very
elevated situations, particularly in tropical region.*, the
amplitude is greater proportionally to the whole pressure
than at lower levels. This is what is to be expected from
the law of radiant heat by which more of the heat rays of
tlie sun is absorbed by the air, and particularly by its
aqueous vapour, mass for mass, in the higher than in the
lower strata.
When the daily maximum temperature is past, and the
temperature ha.-> begun to fall, the air becomes more
condensed in the lower strata, and pressure consequently
at great heights is lowered. Owing to this lower pressure
in the upper regions of the air, the ascending current
which rises from the longitudes where at the time the
afternoon pressure is low flows back to eastward, thus
increasing the pres-sure over tho.se longitudes where the
temperature is no^v falling. This atmospheric quasi-tidal
moveniont occaii.Jin tlie p.m. increase of pressure, which
roachji the luaxiiuuiu from 9 p.m. to midnight, according
C?CII.LATIOXs.]
M E T E O n 0 L 0 Cr y
123
to latit'ide and gcograpliical position. This maximum is
therefore caused by acrcssions to the mass of tlio atmosphere
overhead, contributed by the ascending currents from the
longitudes of the afternoon low pressure immediately to
westward.
As midnight and the early hours of morping advance,
these contributions become less and less and at length
cease altogether, and pressure continues steadily to fall.
But between the time when the increase of pressure from
tic overflow through the upper regions of the atmosphere
ceases and the time when pressure increases from the heat
rays, direct or indirect, of the returning sun, or during the
hours of the night when the effects of nocturnal radia-
tion are the maximum, pressure is still further reduced
t'roni another cause. Eadiation towards the cold regions
cf space takes place, not only from the surface of the
globe, but also directly from the molecules of the air and
its aqueous vapour. The effect of this simultaneous cool-
mg of the atmosphere through its whole height is neces-
sarily a diminution of its tension. Since this takes place
at a more rapid rate than can be compensated for by any
mechanical or tidal movement of the atmosphere from the
regions adjoining, owing to the inertia and viscosity of the
air, pressure continues to fall to the morning minimum.
This minimum is thus due, not to the removal of any of
the mass of air overhead, as happens in the case of the
afternoon' minimum, but to a reduction of the tension or
pressure of the air consequent ujxin a reduction in the
temperature through radiation from the aerial molecules
towards the cold regions of space. In the open ocean the
morning minimum is largest in the equatorial regions, and
it diminishes with latitude ; but the rate of diminution
with latitude through anticyclonic and other regions is
generally less and more uniform than in the case of the
afternoon minimum.
The amplitude and times of occurrence of the phases of
the diurnal barometric tides are subject to great modifica-
tions over the Igind. The amjilitude of the oscillation
from the morning maximum to the afternoon minimum is
greatest where the atmosphere is driest and the sky
clearest, and least where the atmosphere is highly saturated
and the sky more frequently and densely covered with
cloud?, being thus generally the reverse of what is observed
to take jilace over the open sea. The meteorology of India
affords the most striking illustrations of this remark. At
Bombay in April during the dry atmosphere and clear
skies of the north-east monsoon, the oscillation is O'llS
inch ; but in July during the humid atmosphere and
clouded skies of the south-west monsoon it falls to 00G7
inch. In the Punjab, where the air is drier, it is much
greater, rising in excejitional years, such as 18.i2, to 01S7
inch. The much greater amplitude of this oscillation on
land as compared with the oiien sea is entirely due to the
heating of the earth. By this heating of the surface the
lower strata of the air become also highly heated and the
tension is increased ; and, since the air docs not expand
freely, vertically and laterally, from its inertia and viscosity,
the barometer rises. AHien, however, the resistance is
tnercome, the ascending current which sets in is stronger
owing to its higher temperature. Since this liighcr
temperature which has its origin in the superheated
surface is in addition to the direct heating of the air by
the heat fays of the sun as they i>nss through it, the
murning maximum and the afternoon minimum over lanil
.'ire both more extreme than over the ojicn sea. It follows
tliat this oscillation is much larger over land, and largest
ill climates where in.solation is strongest.
In places alreaily referred to where the morning maxi-
juiini is greatly retarded, sueh as Hclder, Sitka, Valentia,
aud Falmouth, the afternoon minimum in the summer
months is singularly small,-»-so small indeed that it does
not fall so low as the mean pressure of the day. This
peculiarity in the diurnal barometric tide is in all prob-
ability due to their insular position to the westward of
a more or less extensive tract of land, by which a tidal
overflow is propagated through the upper regions from tho
continental towards the insular situations. This tidal
overflow receives its impulse from tho a.scending current
from the land, which rises sooner and stronger from inland
than from insular situations. On the other hand, on th-j
open sea, and away from land in regions where the morn-
ing maximum and afternoon minimum are both small, the
minimum always falls below the mean of the day, and the
time of occurrence of the maximum is not retarded as is
the case in insular situations. A map of deviations from
the daily mean pres.sure of the morning minimum in
summer shows, as regards the middle and higher latitudes,
that it is greatest near the sea, and least in inland con-
tinental situations. Indeed in the interior of the Old-World
continent the dip in the curve in the early morning is so
small that the minimum does not fall below the daily mean
pressure, but at most placeJ remains considerably above it.
The same relations are seen in north-western Europe, where
the morning minimum is - 0'020 inch at Valentia and
Falmouth, -0-018 inch at Helder, and -0012 inch at
Amstt:rdam, whilst at Kew it is only - 0'002 in'h. From
its compact form and relatioixs to the surrounding ocean,
the Spanish Peninsula well illustrates the peculiarities of
this phase of the pressure. The deviations from the daily
mean pressure of the morning minimum are at Lisbon
- 0'022 inch and Coirabra-0'011 inch, but at Madrid
in the interior 4- 0'009 inch, — pressure in the last case, just
as happens in the interior of Asia, not faUing so low as- tho
daily mean
The larger mimmum near the sea arises from the higner
temperature there during the night as compared with
more inland situations, from which results a tidal overflow
through the upper regions from the sea towards the land,
as the temperature of the latter falls lower than the sea
during the night. The effect of this overflow is to reduce
the pressure over those regions whence it proceeds and to
increase it in those regions over which it advances, 'the
shallowing of the morning minimum is greatest in the
higher latitudes of continental climates and most complete
at great elevations, where in some cases the minimum
vanishes, — in other words, where the amount of aqueous
vapour is small and the time is short during which no part
of the atmosphere overhead is touched by the sun's rays.
Since the peculiarity is observable in the curves over nearly
the whole continent, appearing even in the low latitudes
of Calcutta and Madias, it might be suggested whether we
have not evidence here of a vast tidal movement propagated
through the higher regions towards that trough-like section
of the atmosphere as it moves westwards over the continent
where the temperature of the lower strata of the air is
about the minimum of the day and pressure also about
the minimum.
Reference has oecn made under Atmospheee to tne
smallness of the range from the x.yi. maximum to the p.m.
minimum in the North Atlantic during summer. This
l>hase in the diurnal distribution of pressure is reju'csentfid
in fig. .3, which shows for .June the mean amount of
the oscillation by hues of 10, 20, 40, 60, 60, and 100
thousandths of an inch, or 0:010 inch, 0-020 inch, ire.
This abnormality begins in March, attains tho maximum
in .June, and terminates in October. It is thus confined
to the warmer months of the year, and, unlike most
meteorological phenomena, is not cumulative, but followj
the sun, so that its maximum occurs in .lune, and not in
July as that of the temperature of the air. or iu August a-i
124
METEOROLOGY
[barometbic OSCILLATIOSa;
the temperatuie of the sea. The smalhiess of this range
over the North Atlantic, which is less than occurs in any
other ocean in the same latitudes, is to a large extent
caused by the small dip in the diurnal curve of the after-
noon minimum.
If the map of the distribi;ition of pressure over the globe
for July be examined (fig. 17) it is seen that this part of
the Atlantic is occupied by a well-defined area of high
mean pressure, — higher indeed than occurs at any season
over any ocean ; and it is shown below that out of this
area the surface winds blow in all directions. But, since
air is constantly being drained out of this region by
the wind without diminishing the pressure, it follows of
necessity that the high pressure must be maintained by
accessions of air received from above through the upper
currents. Now the regions whence such accessions can
come are the upper currents which have their origin in the
ascending currents that rise from the heated plains of Africa,
Europe, the belt of calms, and the two Americas sur-
rounding the North Atlantic. It is evident that the major
portion of each day's overflow of air from the continents
through the upper regions of the air upon the Atlantic,
whether this overflow takes place by convection currents or
from a tidal movement similar to what has been already
described, will take place during mid afternoon. In other
words, the overflow will occur about the time of the after-
noon minimum of the Atlantic, thus diminishing the dip of
this minimum, and so producing the abnormally small range
now under examination. It is in favour of this view that
the abnormality follows the sun's course and is not cumula-
tive, and is felt also on both sides of the Atlantic, even
although the weather on the east side is dry and all but
rainless, and on the west moderately moist and characterized
by a rather copious rainfall. It is also full of significance
that the peculiarity is most strikingly seen in that part
of the ocean of the globe which is closely hemmed in by
large masses of land.
Influence of the Moon on Atmospheric Pressure. — Fifteen
years' hourly observations have been made at Batavia and
discussed by the late Dr Bergsma in their relation to the
lunar day, which was assumed in tjie calculations to com-
mence with the time of the upper transit of the moon. The
result of the inquiry is that atmospheric pressure at Batavia
has a lunar tide quite as distinctly marked as the ordinary
diurnal, baromutric tide, except that its amplitude is much
lei.s. The four phases arc these : —
1st max. -f 0'0022 inch at lunar hour 1
1st luin. -0-0021 ,, ,, ,, 7
2d max. -f 0-0025 , 13
2d min. -00024 „ ,, „ 19
The lunar tide has the important iliiference that its phases
follow the moon's apparent course miich more closely than
the ordinary diurnal fluctuations of the barometer follow
that of the sun. The two maxima occur about the 1st and
13th, and the two minima about the 7th and 19l>h, whereas
these four daily phases of the diurnal barometric fluctua-
tion occur with respect to Jthe sun's apparent course from
one to six hours later. It is interesting to note that in the
higher latitudes in inland situations during \\'inter, or at
times and in situations where the disturbing influences of
temperature and humidity tend towards a minimum, the
times of occurrence of the four phases of the daily o.scilla-
tiou of the barometor approximate to those of the daily
iunar atmospheric tide.
Since a distinct lunar tide is traced to the attractive
influence of the moon, it follows that the- attractive
inlluenco of the sun v.i\\ enter as one of the several causes
■which determine the phases and amplitude of the diurnal
barometric curve. It also follows from the much less
attractive influence of the sun than that of the moon on
the earth's atmosphere that the effects of the sun's attrac-
tion on the pressure -will be wholly concealed by the much
larger effects of the other forces concerned in determining
t)ie diurnal oscillation, except in the case or cases where
the variation in the fluctuation is small at 1 and 7 a.m.
and 1 and 7 p.m. Now at places north of lat. 45*N. the
variation at 1 a.m. is small during the winter, and it is a
singular fact that some years ago Kykatchew of St
Petersburg drew the attention of meteorologists to the
existence at these northern stations of a faintly marked
third maximum ; and it is further of importance to remark
that, at many places where on the-mean of years the third
maximum is scarcely or not at all marked, it appears in
the mean of some of the separate years. Thus, though it
does not appear in the mean of the twenty years ending
1873 at Green-wich for January, it appears in nine of the
individual years. It is highly probable that this maxi-
mum, which may be named Rykatchew's ma.ximum from
its discoverer, is due to the attractive influence of the sun,
its ampUtude and time of occurrence being in accordance
■with such a supposition.
Diurnal Variation of the Force of the Wind. — During
the three and a half years' cruise of the "Challenger,"
ending vrith May 1876, observations of the force anil
direction of the wind were made on 1202 days, at least
AW . . , K PM M
^
b
_
-_
^
^
= ~ ^
^
-
__
-
--
-
-
-
k
^
"7
\
f
—
"" -
y
r
111
-
-
_
1
-Diurnal Force of ■Wind at Sea and i
twelve times each day, — 650 of the days being on the open
sea and 552 near land. The observations of force ^■■er9
made on Beaufort's scale 0-12, being the scale of wind-
force observed at sea. The mean diurnal force of the
wind on the open sea and near laud respectively is showu
WTKD FORCE.]
in fig. 4, where the figures on the left are iJcaulort'.s scale,
and those on the right the equivalents in miles per hour.
The solid line shows at the different hours of the day
the meair force on the open sea, and the dotted line the
mean force near land.
As regards the open sea it is seen that the diurnal
variation is exceedingly small, there being two apparent
slight maxima, about midday and midnight respectively.
On examining, however, the separate means for the North
and South 4tlantic, North and South Pacific, and the
Southern Ocean, there is no uniform agreement observable
among tbcir ciures, the slight variations which are met
with being djJierent in each case. It follows therefore
that the force of the winds on the open sea is subject to
no distinct and uniform diurnal variation. The difference
between the hour of least and greatest mean force is less
than a mile per hour.
Quite different is it, however, ■with the winds encountered
by the "Challenger" near land, the force of the wind
there giving a curve as pronouncedly marked as the
ordinary diurnal curve of temperature. The minimum
occurs at 2 to 4 a.m. and the maximum from noon to 4
P.M., the absolute highest being at 2 p.m. The curves
constructed for each of the five oceans from the observa-
tions near land give one and the same result, or a curve
closely accordant with the curve of diurnal temperature.
The differences between the hours of least and greatest
force are as follows : — Southern Ocean 6} miles, South
Pacific 4i miles, South Atlantic 3J mifes, and North
Atlantic and North Pacific 3 miles per hour.
In the case of each ocean the velocity of the ■mnd on
the open sea is considerably in excess of that near land,
but in no case does the maximum velocity near land,
attained about midday, reach the velocity of the wind on
the open sea. The 650 daily observations on the open sea
give a mean hourly velocity of 17| miles, whereas the 552
near land give a velocity of only 12| miles per hour. The
difference is greatest at 4 a.m., when it amounts to upwards
of 6 miles an hour, but is diminished by the rising tem-
l)erature till at 2 p.m. it is less than 3 miles an hour.
At Mauritius, which is situated within the south-east trades, the
minimum velocity of the wind is 9 '7 miles per hour, occurring from
2 to 8 A.M., from which it rises to the maximum 18 5 miles from
l.to2 P.M., the influence of the sun being thus to double the wind's
velocity. At Batavia, situated in a region where the mean baro-
metric gradient is much smaller, the differences are still more de-
cided. From 1 to 6 AM. 85 per cent, of the whole of the obser-
vations are calms, whereas from noon to 2 p.m. only 1 per cent,
are culms. In all months, the minimum velocity occurs in the
early morning, when the temperature is lowest, and the maximum
from 1 to 8 P.M., when the temperature is highest, the mean
miuimum and maximum velocities being to each other as 1 to 21.
At Coimbra the mean maximum hourly velocit)' is five times
greater than the miuimum hourly velocity in summer, whereas in
wintci- it is only about a half more. At Talentia, in the south-
west of Ireland, one of the windiest situations in western Europe,
the three .summer months of 1878 gave a mean hourly velocity of
13 '3 miles per hour, the minimum oscillating from 10 to 11 miles
an hour from 9 p.m. to 6 a.m., and the maximum exceeding 16
miles an hour from 11 A. M. to 5 p.m. The absolute lowest hourly
mean was 10 miles at 11 P.M., and the highest 18 miles at 1 p.m.,
the velocity about midday being thus nearly double that of the
night. Many observations might be added to these, including
those jmblished by Hann, Koppen, Hamber^, and others, which go
to establish the fact that the curves of the diurnal variation of the
velocity of the wind generally conform to the diurnal curves of
tepjperature. The cun-es are' most strongly marked during the
hottest months ; and the maximum velocity occurs at 1 P.M. or
shortly thereafter, being thus before the time of occurrence of the
maximum temperature of the day, and the minimum in the early
morning, or about the time when the temperature falls to the
lowest. The rule also holds good with all winds, whatever be their
direction. The exceptions to this rule are so few and of snch a
kind that they are probably to be attributed to causes more or
lees of a local character.
Hann has shown, for a number of places in northern Europe, tliat
with a clear sky the velocity is doubled from the minimum to the
METEOROLOGY
125
noaximum, with a sity half covered the velocity is threcfourtha
greater, and with a sky wholly covered the velocity is only a haU
more. On the other hand at the strictly inland situation of Vienna,
with a clear sky the velocity is double, and with a sky half covered
it is two-thirds gieater, bat with a covered sky the diui-nal varia-
tion in the wincTs velocitj- becomes irregular and faintly marked.
Hann has also examined the w inda at Vienna, and found that winds
j of a velocity not exceeding 30 kilometres an hour show a mean
I diurnal increase from 11 kilometres at 6 a.m. to 168 at 1 p.m., but
! that winds of velocity exceeding 30 kilometres an hour exliibit only
! a faintly marked and irregular increase of velocity during the day.
j In offering an explanation of this remarkable fact regard-
I ing the diurnal variation in the velocity of the wind in all
climates, it is to be remarked that the minimum velocity
occurs when terrestrial radiation and its effects are greatest,
but the increase of the velocity closely follows the sun,
and the maximum is reached nearer the time the sun
crosses the meridian than perhaps any of the other maxima
or minima of meteorology which are dependent on the
sun's diurnal course. It is also to be noted that the ivinds
over the open sea are practically vminfluenced by solar
and terrestrial radiation, for there the diurnal curve of
variation in the force of the \\'iiid is all but a straight line.
On Hearing land, however, the wind's force exhibits a
diurnal curve of variation as distinctly marked as, and
bearing a close resemblance to, the analogous curve of
temperature ; while on the land itself these features
become still more decidedly pronounced. Lastly, the
amount of the diurnal variation of the temperature gi the
surface of the sea is less than a degree, whereas over all
land surfaces the diurnal variation of the temperature is
large, even where the ground is covered by vegetation, and
enormously large over sandy wastes.
From this it follows that, so far as concerns any direct
influence on the air itself, solar and terrestrial radiation
exercise no influence on the diurnal increase of the velocity
of the air with the increase of its temperature, — or, if any
influence at all, such influence must be altogether insig-
nificant, as is conclusively shown by the wind observations
of the " Challenger " over each of the five great oceans of
the globe. The same observations show that on nearing
land the wind is everywhere greatly reduced in force.
The retardation is greatest during the hours when the daily
temperature is at the minimum ; and it is particularly to
be noted that, though the temperature rises considerably,
no marked increase in the velocity sets in till about 9 a.m.,
when the temperature has begun to rise above the daily
mean. From this time the increase is rapid (see fig. 4) ;
the maximum is reached shortly after the period of strongest
insolation ; and the velocity falls a little (but only a little)
during the next three to five* hour.?, according to season,
latitude, and position, and falls again to near the minimum
shortly after the hour when the temperature is at the
mean. Even at the maximum, the velocity near land
falls considerably short of the velocity which is steadily
maintained over the open sea by night as well as by day.
The period of the day when the wind's velocity is in-
creased is practically limited to the hours when the tempera-
ture is above the daily mean, and the influence of this
higher temperature is to counteract to some extent the re-
tardation of the wind's velocity resulting from friction and
from the viscosity of the air. The increase in the diurnal
velocity of the wind is in all probability due to the super-
heating of the surface of the ground and to the consequent
ascensional movement of the air, tending to counteract the
effect of friction and of viscosity between the lowermost
stratum of the air and the ground. It is of importance
in this connexion to keep in view the fact that in cloudy
weather a temperature much higher than might have been
supposed is often radiated from the clouds down upon the
earth's surface,' which accounts for the phenomenon of the
' Journal of Scottish Meteorological Societi/, vol. ii. p. 280.
126
METEOROLOGY
[WIKD r-IEECTIuS,
diurnal rariation in the wind's volocity occurring frequently
also in cloudy vrcather. On the other hand, during the
night, when terrestrial radiation is proceeding, the tempera-
ture of the surface falls greatly, and instead of an
ascensional movement in the lower stratum of the air there
is rather a tendency towards a descensional movement (if
the wind be light there is an actual movement) of the
lowest air stratum down the slopes of the country ; and
since the friction between the wind and the surface of
the earth is thereby increased the diurnal velocity of the
wind falls to the minimum during these hours (see also
p. ISG).
Among the most marked exceptions to the general rule
of the diurnal distribution of wind force may be cited the
bitterly cold furious blasts of wind encountered in narrow
valleys in such mountainous regions as the Alps during
clear and comparatively calm nights. These are simply
the out-rush of the cold air poured into the upper basins
of the valleys by the descensional currents from the slopes
which the chilling effects of ■ terrestrial radiation set in
motion. On the other hand; the air of the valleys becomes
jheated and expands during the day, thus giving rise to a
[Warm wind tilowing up the valJeys, which, on accoimt of
the vapour it carries with it from the lower levels, fre-
quently covers the higher slopes and tons of the mountains
with cloud and drizzling rain.
Diurnal Variation in the Diredi/m of tlie Wind. — In all
climates near seas and other large sheets of water, where
the distribution of atmospheric pressure is tolerably equable,
or the barometric gradient small, and the sun heat
moderately strong, land and sea breezes are of daily
occurrence. In such places a breeze from the sea gradually
sets in in the morning, which gradually rises to a stiff
breeze during the heat of the day and again towards
evening sinks to a calm. Soon after this a breeze sets in
from the land, blows strongly seaward during the night,
and dies away in the morning, giving place to the sea
l^reese as before. These breezes are occasioned by the
fciurface of the land being heated in a much higher degi'ee
than that of the sea during the day ; the air over the land
being thereby made lighter ascends, and its place is
supplied by the cooler air of the sea breeze drawn land-
ward, and parti}' also by descending currents, as shown
by the humidity observations of the " Challenger," which
indicate increasing dryness when the sea breeze is strongest.
Again during the night the temperature of the land and
of the air over it falls below that of the sea, and the air of
the land thus becoming heavier and denser flows over the
sea as a land breeze. As the best-marked and most fre-
quently occurring cases of the sea breeze begin some
distance out at sea and gradually approach the land, it is
veiy probable that, as suggested by Blanford, the ascend-
ing heated air flows seaward as an upper current, and that
the increased barometric gradient thus caused largely
accounts for these breezes.
Sea and land breezes are tlma determined by the relative posi- .
tions of the land and its coasts, subject to a further modificatiori '
arising from the rotation of the earth, Tims on the coast of the '
Gulf of Lyons the sea breeze from the south veers to sonth-west '
and dies away as a west wind, while the land hicczo from tlie north '
gradually veers to nortli-east and dies away as an cast vnnd. On [
flic coast of Algeria, on the other hand, the sea brep/e veers from I
north to north-east and dies away in the east, whereas the south '
land breeze veers to south-west and dies away in tlie west. Sea '
breezes also occur iu such unsettled climates as that of Scotland, I
when the weathoj conditions arc favourable. These conditions are
presented when an anticyclone overspreads the country, with its
accompanying fine settled weather, small variation in the distri-
bution of atmospheric pressure, clear skies, and consequently strong I
tunshine. Under these conditions the following are trie vecriuf:^ of I
the wind off the coast of Berwioksbiro. Iu tlie momiug the wind is |
north- wcit till about .10 A.ii., when it veers to north, falling all tlio i
time til] finally it sdnke to a calm. A little before noon it springs up
from north-east or ca<it, veal's to south-east from 2 to a p.m., where
it continues till 7 p.m., about which time it veers to south aud theQ
south-west, diminishing in force and finallysinking to a calm. Alwut
sunset it springs up irom west, veering to north-west during tlic
night, where it continues till tlie following morning. The wind thus
virtually makes the round of the compass, is strongest from north-
west and south-east and weakest at north-east and south-west, being
thus strongest when its coui-so is perpendicular to the line of coast.
The observations made by the " Challenger " in the i-emon of the
north-east trades in 1873 show a small diunial variation in the
direction of the wind, the variation being from E. 47" 5' N. at 2
to 6 A.M. to E. 56" N. at 10 a.m. to 2 p.m., the variation being
thus 8" 55' towards north durinof the hottest hours of the day. At
Mauritius observatory, wliich is several miles from the sea, tha
daily period in the direction of the wind is from E. 22° 15' S.
at 4 A.M., being the most southerly point, to E. 7^ S. at I P.M.,
and thence back to E. 22° 15' S. at 4 A.M. Tlie diurnal varia-
tion is 15° 15', and thus the hifluence of the sun imprer,se3 on tho
wind at this observatory a more truly easterly character.
At the Austrian naval station at Pola, near the head of the
Adriatic, the daily variation in the uirection of the wind ia weli-
markei Starting from a point eait of south at 5 a.m., it gradually
veers round to westward, the most westerly point, almo.st due west,
being reached at 5 to 6 p.m., after which it gradually shifts back to-
ils starting point in the morning. Here we have evidently a diarzial
wind-system different from that of the land and the sea breeze.
Pola is situated near the south-western extremity of the peninsula
of Istria, and the direction in the early morning of east by south in
the direction the wind would take if a small anticyclone oversjH-ead
the peninsula ; and the direction from the west iu mid afternooQ
is the direction the wind would have at Pola if the peninsula weru
occupied by a small cyclone with the lowest pressure in the centre.
Now the influence of solar radiation is to form, through ths
ascending current from the heated land, a diminution of i>ressure
over the land, — in other words, what is essentially a cyclone. On
the other hand, during the night the influence of terrestrial radia-
tion is to generate, through the cooling of the laud and the air
resting above it,- a relatively higher atmospheric pressure iu tho
interior of the peninsula with its characteristic system of out-
blowing winds. ^
At Coiuibra, in July 1878, the diurnal variation of the wind's direc-
tion was from W. 49° 37' N. at 2 to 6 a.m. to W. 33' 16' N.
at 4 to 6 P.M., the amount of the variation being thus 16" 22* in t!io
direction of west. At Valentia, in the south-west of Ireland, durin.^
the summer months of 1878 the diurnal variation of tho wind's
direction was from W. by S. at 7 to 9 a.m. to S.W. by
W. at 5 to 7 p.m. The variation was thus from a point nearly
south to a point nearly south-west, or through nearly 45*
in tho direction of west On tho otlier hand, at Al>erdeen
during the same months of 1878, the diurnal variation of the
wind's direction was from S.W. at 6 to 7 a.m. to S. by E. at 12
to 4 P.M., the variation being thus 56" from south-wciit iu the
direction of east through south. Attention is here drawn to tbo
exactly opposite ways \n which the diurnal veering or shifting of
the wind takes places at Valentia and Aberdeen, hut i>articularly to
the important circumstance that in each case the diunial changes
in the wind's direction which actually occur ai-e precisely ihase tliat
would take place on the supposition that during the hottest Ituura
of the day an ascensional movement of the air sets in from tho
heated lands of the British Islands, and that an in-di-au'^ht takes
place all round, wluch with the descending currents makes good
the loss caused by the up-draught. Thus then both the diurnal
increase in the wind's velocity and the change in its direction
which observation shows to take place during the hottest -hours of
the day are traced to tho same cause, viz., the heating of tho
sm'faee by the sun, the licating of the lowest stratum of air resting
on the surface, and the ascensional movements which are tho neces-
sary result.
It is instructive to note that at Nukuss, at some distance to the
south of tho Sea of Aral, where the summer direction of tlie wii.-l i.-i
northerly, tho north component is at the daily maximum at 4 p.m.,
having shifted into this direction from north-east, where it is at
9 A.M. Much or nearly cvorytliin^ remains to bo done in working
out this problem in its practical details as one of the imiM>;tant
elements of climatology, with tho view of airiviug at some doliuit«
knowledge of tho influence of physical configuration and dilferent
vcffetahle coverinpa of tho surface ou radiation and on the velocity
and direction of the wind.
Diurnal Variation in tJte Amount of Cloud. — ^lists and
fogs are visible vapours floating in the air near tho surface
of the earth, and clouds are visible vapours at a cousider-
able height. These fonns.of visible vapour are all produced
by wliatever lowers the temperature of the air below the
dew point, — such as radiation from the molecules of the
atmosphere towards the cold regions of space, the simpl*
CLori).]
METEOROLOGY
127
expansion of llie air of ascending CTirrerits, the mixing of
cdld air iritli air that is warm and moist, and tlie cooling
of tlie air in contact with tlie surface of the caith when its
tcmperaturo has been lowered by nocturnal radiation.
The forms of clouds are endless. Since clouds are
subject to certain distinct modifications from the same
causes which produce other atmospheric phenomena, the
face of the sky may bo regarded as indicating the operation
of these causes, just as the face of man indicates his mental
and physical states. Hence the importance of the study
(if clouds, and hence the necessity of a nomenclature of
clouds as the basis of accurate and comparable observations.
Ah adequate nomenclature of clouds is still a desideratum.
Luke Howard's classification, which continues to hold its
ground as a provisional nomenclature, was proposed ■ by
him in 1803, and by it clouds are considered as divided
into seven kinds. Of these, three are simple forms, the
cirrus, the cumulus, and the strattis ; and four intermediate
or compound, the cirro-cumultis, the cirro-stratui, the
eumulostratus. and the aimulo-ctrrostratm, nimbus, or rain
tlovd.
The cirrus cloud consists of wavy, parallel, or divergent
filaments, which may increase in any or all directions. It
is tile cloud of the least density, the greatest elevation, and
the greatest variety of figure. It is probable that the
liarticles composing it are minute crystals of ice or snow-
tlakes. The cirrus is intimately connected vriih the great
movements of the atmosphere ; and it is solely from the
movements of the cirrus that we have any direct know-
ledge .of the upper currents of the atmosphere. In recent
years much has been done, particularly by Professor
Hildebrandsson of Upsala and Clement Ley, in investi-
gating the relations of this cloud to storms and other
changes of weather.
The cumulus is the name appuea to those convex or
conical heaps of clouds which increase upwards from a
horizontal base. They are generally of a very dense
f.tructure, are formed in the lower regions of the atmo-
sjihere, and are carried along by the aerial current next
the earth. They form the tops of the ascending currents
which rise from the heated ground, and have a diurnal
period so well marked that they are often named the
"cloud of the day." The form of stratus comprehends'
those mists and fogs which in the calm evening of a warm
summer day make their appearance in the bottom of valleys
and over low-lying grounds, and sometimes spread upwards
ovei the surrounding country like an inundation ; they
have an equally well marked daily period, and are
frequently called the "cloud of night.'' The cirro-
cumulus is made up of small roundish masses, lying near
each other, and quite separated by intervals of sky. It
may be considered as formed from the cirrus by the fibres
of tha. cloud breaking, as it were, and collapsing into
roundish masses, thus destroying the texture but retaining
the arrangement of that cloud. This singularly beautiful
cloud is commonly known as a mackerel sky, and is of
most frequent occunence during dry warm summer weather.
The cirro-stratus consists of horizontal masses thinned
towards the circumference, bent downwards or undulat-
ing, and either separate or in groups. Since this cloud
lias great extent and continuity of substance, but little
perpendicular depth or thickness, it is the cloud which
most frequently fulfils the conditions for the phenomena
of coronae, solar and lunar halos, parhelia or mock suns,
and paraselenie or mock moons. The cumulo-stratus
is formed by the cirro-stratus blending with the cumulus,
or spreading underneath it as a horizontal layer of vapour.
Tke cumulo-cirro-stratus, or nimbus, is the well-known
laincloud, which consists of a cloud or system of clouds
iiom which rain is falling. At a considerable height a
sheet of cirro-stratus clond is extended, unacr whfcfi
cumulus clouds drift from windward ; these rapidly in*
■ creasing unite and appear to foiTn one continuous grey
mass from which the rain falls. ' The breaking up of the
lower grey mass indicates 'that the rain will soon cease.
■When a rain-cloud is seen at a distance, cirri appear to
shoot out from its top in all directions; and it is observed
that the more copious t'lo rainfall the greater is the dis-
play of cirri. The cirrus, cirro-cumulus, cirro-stratus,
cumulo-stratus, and nimbus are connected more or less
closely with the great atmospheric movements of the
cyclone and anticyclone. In what follows here only the
amount of sky covered will be taken into account, and not
the .species of clond covering.
The diurnal variation in the amount of cloud in the sKy
on the open, sea is very small. •' The following are the means
of two hundred and seventy-seven days' observations on
board the " Challenger," stated in percentages of sky
covered : —
2 a.m. 59 10 a.m. tii) I 6r.M. 57
i „ 69 Noon 56 ! 8 „ 67
a „ 62 2 P.M. 58 I 10 „ 67
8 „ 62 „ 59 I Midnight 57
Two maxima are here indicated, the one about or shortly
after sunrise and the other in the early part of the
afternoon ; and two minima, the one at noon and the other
from sunset to midnight. The difference between the
extremes is only 6 per cent, of the sky.
At Batavia the daily maximum is from 6 to 11 P.M., and the
minimum from 8 to 11 a m., the extremes being 52 per cent, at
9 a.m. and 69 per cent, at 7 P.M., — a difference of 17 percent. Of
four daily observations at Mauritius, the maximum is 50 per cent,
at 1 P.M. and the minimum 38 per cent, at 6 a.m. At Cpimbra,
obstrvations of clouds have been made five times daily, and six
years' results give the maximum 63 per cent, at 9 p.m. and the
minimum 62 per cent, at 9 A.M. At this place, during July and
August, the greatest amount of cloud occurs at 6 P.M., and in these
months the rainfall at Coimbra is very small. The minimum is
more pronounced at 9 a.m. than at any other period ; in winter
tliis (ihase occurs about four hom-s later. At the continental
situation of Vienna, during the warm months of the year the maxi-
mum is at 2 P.M., with a secondary maximum about 6 A.M., and
the minimum from 10 P.M. to 2 a.m. ; but dm-ing the cold months
the maximum is at 6 a.m. and the minimiim during the evening
and night. In the Rocky Mountains, the chief maximum, 57 per
cent., is at 3 p.m., with a secondary one 30 per cent, at 5 A.M.; and
the chief mininmm 20 at 3 A.M. and a secondary one 29 at 11 P.M.
At Ilelbiiigfors the maximum of cloud occm"sfrom 10 a.m. to 2 P.M.,'
and the minimum from 10 P.M. to 2 a.m.
Much yet remains to be done with regard to me
determination of the diurnal variation of cloud, but from
the above one or two deductions of a general character
may be drawn. A maximum occurs in the rnorning and
continues till shortly after the sun has risen, and this
maximum is more decidedly pronounced over the open .sea
than over land. Its appearance is without a doubt due to
the general cooling of the atmosphere through its whole
height by terrestrial radiation, and its disappearance to
the heating of the air, which commences about sunrise.
Then follows one of the diurnal miruma, which continues
till midday, or a little later ; in other words, it continues
till, owing to the diurnal heating of the aii- by the sun,
the ascending current has fairly set in. The period of
this ascending current marks the second maximum, which
during the warmer months is larger than the morning
maximum over land. The cumulus is the characteristic
cloud of this maximum. These clouds are merely the
summits of the ascenditig currents which rise from the
heated land, where the aqueous vapour is condens,ed in
cloud by the expansion which takes place with increase of
height.
These cumulus clouds throw a not unimportant iignt on
the behaviour of the ascending currents which rise from
the surface when heated by the sun, — inasmuch as they
128
:\I E T E 0 R O L 0 G Y
[diuhxal p.^infalc.
point to the fact that tlie ocrrent ascending from Iho
surface is broken up and thereafter grouped into sciiarate
well-detincd a:jcending currents, which are marked out and
overtop|)ed by these cumuli ; and further it is probable,
from thoir well-defined position, that the air composing
the ascending currents is not only warmer but also more
humid than the air in the clear intei-spaces at the same
heights. It may also be regarded as highly probable that
it is down through these clear interspaces that the descend-
ing air-filaments shape their course in their way to take
the place of th& air-molecules that ascend from the heated
surface of the earth.
The secondary minimum occurs from about sun.set
onwards during the time of the P.M. maximum of atmo-
.spheric pressure. In a highly .-iaturated atmosphere, which
is so characteristic a feature of many tropical climates at
certain .seasons, this lime of the day is remarkable for the
amount of cloud; and it is during those seasons and hours
that huat-lightning, or lightning without thunder, attains
its annual and diurnal maximum period, which is from six
to eight hours later than that of thunderstorms. The
morning maximum, j-hortly before and after sunrise, has
two quite distinct and characteristic clouds accompanying
it. One of these is the curaulo-stratus, which is a con-
sequence of the cooling of the atmosphere through all its
height by nocturnal r.idiation. As the colouring of the
cloudlets is often singularly fine, it has been a favourite
theme with poets of all ages and climes. The other, which
results from the cooling of the surface of the earth by
terrestrial radiation and thence of the lower stratum of
the atmosphere, is quite different, being a low creeping
mist, appearing first in low-lying situations, and gradually
extending upwards as the temperature falls. Fog is a
well-kno\ra form of this cloud, having its diurnal maximum
in the morning and early part of the day.
Dill null Variation in the Amount of the Bain/all. —
From the sLxteeu years during which hourly observations
of the rainfall were made at Batavia Dr Bergsma has given
a table showing the diiu-nal variation, of which the follow-
ing shows how much per cent, of the total daily amount
fell e\Lry two hours : —
Midt. lu'2 .i.M. 8-7 I 8 A.M.tolO A.M. .1-5 i 4 P.M. toO r.M. 13-5
2 a.m. „ i „ 0-4 10 „ „ Noon 6-3 6 „ „8 „ 10-5
4 „ ,, G „ 6-1 , Noon „ 2 P.M. 95 i 8 „ „ 10 „ Ti
« „ „8 „ 6-2 I 2 P.M.,, 4 „ 12-2 1 10 „ „ Midt. 87
The diurnal curve of rainfall is thus very distinctly
marked at Batavia. The minimum is from 6 to 10 a.m.
and the maximum from "2 to 6 P.M., — 10"7 per cent, falling
during the four hours ending 10 A.M., but 25'7 per cent,
in the four hours ending 6 P.M.
Thu observations ut-ie arranged and averaged by Dr Berganja
with the view of seeing liow far the pliases of the moon influence
the rainfall. The results for the eight phases of the moon,
beginning with new moon, showing tiie mean amount of rain in
t\venty-four liours during the seventeen year.s ending 1880, are
these :-0"243, 0-236, 0193, O'lSl, 0-212, 0-183, 0-189, and 0-203,
and daily mean 0-205 inch. The influence of tlic moon's pliascs
on the rainfall at liatavia is thus quite decided from tliese seventeen
years; for, while tlie moan daily rainfall is 0-20.-5 inrh, it rises at
full moon to 0-243 incli, from uhich time it gradually falls to
0-181 inch at the tliird octant, rises to 0-'212 inch at the fourth
octant, falls again to 0-183 inch at the fifth octant, and finally
rises to the maximum at the time of new moon.
At Coimbra, where the rainfall has' been observed every two
hours for the six years ending 1881, the moans show a minimum
of 8-08 inches from midnight to 2 a.m., a maximum of 4-03 inches
from 2 to 4 a.m., a second minimum of 3-20 inches from 10 a.m.
to noon, and a second maximum from 2 to 4 P.M. These four
phases of the rainfall are i pretty nearly accordant with the font
phases of the barometric pressure, the maximum periods being
near the times of minimum pressure,, and the minimum periods
near the times of maximum i>ressure. The rainfall at Philadelphia
shows a ilecided Qjaximum at 0 P.M. and miniuniin at 3 4.M. At
Vienna during the siiuinu-r half of the year there are three maxima
and three niiuinia in the curve uf the daily rainfall, the chief
maximum, which is nearly double of each of the other two,
oi-eurring from 2 to 4 P.M., and the chief minimum from 3 to 6
A.M. At this place the number of hours of rain kas been recorded,
shov.ing two maximum periods, the first from 2 to 8 A.M. and the
second from 4 to 7 p.m. Since the time of maximum amount
indicates a nuniber of hours for the fall under the mean of the day.
it follows that the showers from 2 to 4 p.m. hk often very heavy.
At Prague the chief maximum is from 2 to 6 p.m. and the minimum
from 1 to 0 A.M. At Zcchen the maximum is from 2 to 7 p.m.,
with a secoiulary maximum from 5 to 8 a.m., and the minimum
from midnight to 4 a.m. At Hern the maximum fall is from 7 p.m.
to midnight. Twenty-one years' observations at Calcutta show
the maximum occurrence of lainfall during the raijiy season from
June to October to be from 11 a.m. to 6 p.m., the absolute maximam
being from 2 to 3 P.M. and the minimum from 9 p.m. to 1 A.M. ;
and during the hot dry season from March to May the maximum is
from 5 to 9 P.M., and the minimum from midnight to 9 a.m.
The data already collected .show the general occurrence
of a diurnal maximum from about 11 a.m. to 6 p.m., and
this feature of the curve is particularly well seen in the
rainfall of continental climates during the summer half of
the year. A marked diminution of the rainfall is very
generally observed from about sunset to midnight, when
the diurnal amount of cloud in many climates falls to the
minimum, and the evening maximum of atmospheric
pressure takes place. The time of the morning minimum
pressure from about 2 to G a.m. is, curiously, strongly
marked in some places with an increase, while in others it
is as strongly marked with a diminution, in the rainfall.
I'he " Challenger " observatioms show that the occurrence
of rain on the open sea is inversely as the temperature,
68-1 da}s' observations giving 96 cases from 9 to 4 p.m.,
and 135 from midnight to 2 a.m.. these being the miaimuin
and maximiun periods.
Diurnal Variation of Thioulert-torms. — It has just been
remarked that a prominent feature of the diurnal rainfall
in continental climates during the summer months is the
increased rainfall from about 11 a.m. to 6 p.m., and the
Vienna observations point to unusually heavy falls occur-
ring at these hours. This is caused by the rains which
accompany the thunderstorms of these regions. The
following table gives for the hours of the day the times of
occurrence of thunderstorms at Ekaterinburg in the UraJ
Mountains during the fourteen years ending 1872 : —
Apul.
May.
Jane.
July.
AUE.
Scpi.
YMr.
Midnig' ^ to 1 a.m
5
5
16
1 A.- 2 „
1
2
8
2 „ „ 3
...
1
1
6
3 ,, „ 4
1
3
6
4 „ „ 5 „
2
1
4
G „ „ 6 ,
3
B
6 „ ,,7 ,
2
5
7 „ „ a
i
6
2
10
8 ,, „ 9 „
1
4
1
10
9 ,, „ 10
1
6
6
19
10 „ „ 11
1
8
12
4
25
11 „ „ Noon
1
2
14
30
5
1
63
Noon „ 1 p.M
3
4
19
25
5
4
60
1 P.M. ,, 2
2
«
21
29
12
2
74
2 ,, ,,3
3
10
22
35
15
4
89
3 ,, „ 4
3
6
2£
45
20
1
101
4 „ ,,5
' 2
5
24
33
9
73
i „ ,,6
1
6
m
30
11
2
75
6 „ ,,7 „
2
7
l&
20
10
...
54
7 ,, „ 8 ,
2
5
18
20
9
52
8 „ „ 9 „
2
6
14
14
6
42
!) „ „ 10 „
2
3
8
10
5
1
29
10 „ „ 11
1
G
5
18
11 „ ,, Midnight...
1
7
8
22
Sums
27
64
255
SSI
144
16
856
Hence the thunderstorms at this jilace have a diurnal
period as strongly marked as any other meteorological
phenomena, and in this respect Ekaterinburg is fairly
representative of extratropical continental climates during
summer. For the fourteen years no thunder occurred
THtTNDEBSTOEMS,]
METEOROLOGY
12i»
during the six months from October to March. The mean
of the six hottest months shows the maximum to take
place from 3 to 4 p.m. and the minimum from 4 to 5 am.,
these being the times of occurrence of the two minima of
pressure. At this season, however, the morning minimum
pressure is but faintly marked in such climates as those of
Siberia. During the twelve hours from 9 A.M. to 9 p.m.,
when the temperature b above the daily mean, 717 of the
whole number occurred, thus leaving only 139 for the
twelve hours when the temperature is below the daily
mean. The great majority of the thunderstorms occur
during ths part of the day when the ascensional movement
of the air from the heated ground takes place, and they
attain the maximum when the temperature and this
upward movement are also at the maximum. Owing to
the westerly winds from the Atlantic which prevail over
Europe and western Siberia during summer, the maximum
rainfall of the year occurs over this extensive region in this
season ; and the importance and significance of the inquiry
into this element of climate lie in the fact that the g?eater
portion of the summer rains is discharged over these regions
by the thunderstorm. The " Challenger " observations on
the open sea show the maximum occurrence of thunder-
storms to be from 10 P.M. to 8 a.m., 22 being observed
during these ten hours and 10 during the other fourteen
hours of the day, — a result which suggests that over the
ocean terrestrial radiation is more powerful than solar
radiation in causing vertical disturbances in the equilibrium
of the atmosphere.
Atmospheric vapour and ascending currents thus play
an important part in the history of these thunderstorms.
Where the climate is dry and rainless, Like that of Jerusalem
in summer, thunder is altogether unknown. On the other
hand, where during a particular season an anticyclone with
its vast descending current in the centre remains over a
regiQU, as happens over the centre of the old continent
during the winter, over that region thunder is equally
unknown during that season. Further, in such places as
Lisbon and Coimbra, where the summer rainfall is small
and its occurrence infrequent, thunderstorms become les^
frequent, and the hours of their occurrence are later in the
day than they are before and after the dry season.
The thunderstorms at Mauritius call for special notice. There
ire two maxima in the diui'ual curve, the larger from noon to 4
P.M. and the smaller from 3 to 6 A. M., which are near the times of
the barometric minima ; and two minima, from 9 P.M. to 1 A. M.
and from 8 to 10 a.m., these being near the times of the barometric
maxima. But the important point as regards the thunderstorms
of Mauritius is that for twelve yeai-s none were recorded in Juno
and July, one only in August, one in September, and three in
October. The annual period of the thunderetorms of this island
extends from near tlie end of October to the middle of May, or
during the time of the greatest rainfall, practically noue occurring
during the rest of the year. But rain contiuues to fall during
the four months of no thunder, the mean monthly rainfall being
then about 2 inches, falling, ^ however, in September to 1*37
inches. During these four months, therefore, there is in the air
the a((ueous vapour, and, these being dry months, there is the
condition of ascending cmrcnts. There appears, however, to
be then wanting another element which seems essential to
the electrical manifestations of the thunderstorm, viz., the con-
ditions which give masses of descending cold air along with
the ascending current of warm moist air. Buring the months
when thunder is of no unusual occun-ence the high pressure of Asia
repeatedly advances, as Dr Meldrum has pointed out, close on
Mauritius ; and so frequently is this the case that he considers the
belt of calms bet^vcen the two trade winds to stretch in a slanting
direction from Madagascar to Ceylon. As long as this state of
things occurs with more or less frequency, the conditions of a
descending cold current of large volume are provided, and thunder-
storms occur. But during June, July, August, and September,
when atmospheric pres.=ure is low in Central Asia, and there is an
unbroken increase of pressure from Asia southwards to Mauritius,
and while Mauritius remains in the heart of the south-east trades,
the condition? of descending cold currents of any conflidcrable
Tolmne ar« not present, and thu::dcr is there unknown at that
season. °'
Now in situations which afford the three conditions of aqueooa
vapoiir, ascending currents, and descending cold currents, whilst
the diurnal and annual periods are quite aistinctly marked, the
phenomena are more uniformly distributed through the hours of the
day and months of the year than elsewhere. Pola and Fiuhie, at
the head of the Adriatic, being shut iu and'eucompassed by lofty
Alps, are illustrations. Ac Fiume the greater maximum occui-s
from 11 A.M. to 1 P.M. and the smaller from 2 to 4 A.M., aud the
minima from 10 P.M. to 1 A.M. and 5 to 9 A.M. While during the
twelve hours the temperature is above tlie mean of the day froni
May to September the number of the thunderstorms here was 245
for the nine years ending 1879, the number during the twelve
hours the temperature is under the mean was ISj. The compara-
tively large number during the colder hours of the night is no ooubt
due to the warm moist atmosphere of tliis confined sea aud tiio
close proximity of the Alps.
There is still another set of condition? favoniing the develop-
ment of thunderstorms in certain climates vhich the observations
made at Stykkisholm in the north-west of Iceland illustrate.
During the fourteen years ending 1879 there occurred here twenty-
three thunderstorms, but there was only one in the six warm
months from April to September ; in other words, the thunder-
storms of this climate are essentially winter phenomena. Further,
of the twenty-three hours in which they occurred, only three were
at a time of the day wlien the sun was above the hoiizon, viz.,
twice in March and once in September ; in other words, the thunder-
storms of Stykkisholm are nocturnal phenomena. It is instructive
to observe that in the north and north-west of Scotland thunder
occurs most frequently during the night and in winter, whereas in
central, southern, and eastern districts it occui-s most frequently
during the day and in summer, — the thunderstorms in the former
case approximating in type to those of Icclaud and in the latter
to those of £katerinbnrg. A little reflexion shows tliat in north-
western Europe it is during winter and during night that warm
moist ascending and cold dry descending currents are most fre-
quently brought into close proximity during the great Atlantic
storms of the season; and it is at the changes of wind, humidity,
aud temperature accompanying the passage of the centres of tho
cyclones that the thunderpeals arelieari On the other hand,
in the east and south of Scotland it is during the hot months
of the year that these ascending columns -of warm moist air and
descending columns of cold dry air are most frequently brought
together, and there, accordingly, thunder with tne heavy raina
which accompany it is of most frequent occurrence from 11 A.M.
to 6 P.M. from May to September Tnese essentially different typej
of thunderstorms have been classed by Mohn as heat thunderstorms
and cyclonic thunderstorms.
Given an initial difference of electric potential, it is easy
to understand from the effects which follow the sudden
extraordinary condensations of the aqueous vapour that
take place how the most violent thunderstorms are pro-
duced. The difficulty is to account for the production of
the initial difference of electric potential, — how, for
example, in the same great aerial current of the south-west
monsoon, this difference of potential is produced in the
molecules of aqueous vapour at Calcutta but not in the
aqueous vapour at Maiuitius. It is to the physicist that
meteorologists still look for the explanation.
Diurnal Period in the Occurrence of the Whirlwind,
Waterspout, Diist Storm, and Tornado. — Whirlwinds,
waterspouts, dust storms, and tornadoes are essentially the
same, differing from each other only in their dimensions,
their intensity, or the degree in which the moisture is con-
densed into visible vapour, while the hailstorm and the
rainstorm are simply the manner and degree of the pre-
cipitation accompanying them. In several important
respects they differ widely and radically from cyclones (see
Atmospitere, vol. iii..p. 33). The largest tornadoes are
of so decidedly smaller dimensions when compared with
the smallest cyclones as to admit of no shading of the one
into the other. Cyclones occur at all hours of the day
and night, whereas whirlwinds and tornadoes show a
diurnal period as distinctly marked as any in meteorology.
Finally, cyclones take place imder conditions which involve
unequal atmospheric pressures or densities at the same
heights of the atmosphere, due to inequalities in the
geographical distribution of temperature and humidity ; but
whirlwinds occur where for the time the air is unusually
warm or moist, and where consequently temperature and
rVL — 17
130
METEOROLOGY
[whirlwinds AS1>
humidity diminish with height at an abnormally rapid rate.
Cj'clones are thus phenomena resulting from a disturbance
of the equilibrium of the atmosphere considered horizon-
tally, but whirlwinds and tornadoes have their origin in a
vertical disturbance of atmospheric equilibrium.
Among tbe iriost remarkable of the tornado-swept regions of the
globe are certain portions of the United States ; and to the examina-
tion of these the meteorological service of tlio St^ites has given
special attention by a systematic, careful, and minute observation
(a the attendant phenomena and the destructive effects. Tlie
tornadoes of the last eighty-seven years, numbering about six
hundred, have been classed under the different States where they
Are reported to have occurred, and fig. 5 shows this relative distribu-
tion over the States. The areas of greatest frequency are at long-
distances from each other. That part of the jffreat basin lying
west of the Mississippi, including the States of Iowa, Missouri,
Kansas, and Nebraska, is the region in which tornadoes are most
frequent. Tornadoes - occur at all seasons, being most frequent,
however, from April to September, and least frequent in Decemher
and January.
The hour of occurrence of one hundred and sixty-two of the
tornadoes is given in the official report as follows : —
Midt. ta 2 A.M.
2 A.M.
8 A.M. to 10 A.M.
Noon 7
Noon ,, 2 r.M. 13
2r.M. ,, 4 „ 47
4 P.M. to 6 P.M.
for temperattu*, wind velwity, and thunderstorms. The atmo-
spheric conditions whicli appear invariably to precede the formation
of the tornado are violent contrasts of temperature and humidity
immediately to the north and south of the patli to be traversed by
the storm. It is highly interesting to observe from fig. 5 that the
legion of most frequent occurreucc of tornadoes is the region
wliere a large number of the cyclones of the United States appear
to originate (and the same region Loomis has shown to be remark-
able for violent contrasts of temperature occurring within limited
spaces and times), and that, as appears in th? regions of the
Alleghanies, they decrease in frequency with height.
Fig. 6 shows the waterspout in different aspects. A
black cloud covers the sky, from which a projection is let
down in the form of an inverted cone, as at A, which
continues to increase and extend downwards. The sed
immediately beneath is soon thrown into violent agitation,
showing that the whirling movement which began in the
clouds has e.ttended to the sea, and is doubtless continuous
throughout, though the portion of the column from A
downwards is not yet made apparent by the condensation
of its contained vapour into cloud. As the whirling move-
ment of the column becomes more intensely developed, the
increased rapidity of the fg-rations lirings about increased
rarefaction of the air within, with tlu inevitable result of
increased condensation of the vapour into cloud downward.
The protrusion of the cloud and it.s extension downwards
are thus not due to the descent of vajiour from the clouds,
but to the visible condensation of the nvpour of the spirally
ascending air-currents arising from an increasing rarefac-
tion dtie solely to tie accelerated rate of the gyrations, the
condensation being analogous to that of the cioud seen in
exhausting an air-pump.
Under each of the columns of fig. 6 the surface of tho
sea is seen to be more or less heaped up, as well as in
violent agitation, showing that atmospheric pressure
immediately under the gyrating columns is less than it is
all round. On land, when the tornado passes directly
over a dwelling house or other closed building, it often
happens that the whole building, walls and roof, is thrown
outward with great violence, the wreckage presenting the
appearance of a sudden explosion, proving that atmospheric
pressure outside the building was instantaneously and
largely reduced, and the building shattered to fragments
by the expansion of the air within. It is in this way that
the tornado does some of its most dreadful work.
The wind of the tornado reaches a velocity probably
never equalled in cyclones. During the Ohio tornado of
February 4, 1842, large buildings were lifted entire from
their foundations, carried several rods through the air, and
then dashed to pieces, some of the fragments being carried
distances of 7 and 8 miles ; and large oaks nearly 7 feet in
girth were snapped across like reeda. This tornado swept
on its course at tbe rate of 34 miles an hour, and at oae
TOBKADOES.]
METEOROLOGY
131
riace did its fearful work in the brief space of a minute.
The tornado which passed over Mount Carmel (Illinois),
June i, 1877, swept o2 the spire, vane, and gilded ball of
the Methodist church, and carried it bodily 15 miles to
north-eastward. The velocity of the ascending currents
which kept this heavy object suspended in the air for 15
or 20 miles must have been very great.
Of the tornadoes the progressive courses of which were
recorded, 310 advanced towards N.E., 38 towards S.E., 16
towards E.N.E., 14 towards E., 7 towards N.N.E., 5 towards
E.S.R, and 3 towards S.S.E. The course is thus always
Fio. 6. — Forms of 'Watcr.^'Outi.
towards some easterly direction, the great majority being
Kjwards the north-east. The velocity of their onward
movement varied from 1 2 to 60 miles an hour, the average
being 30 miles an hour. The time occupied in passing a
particular spot varied from 10 seconds to half an hour,
the mean time being nearly six minutes and a half. The
width of the path of destruction marked with debris and
other relics of the violence of the tornado varied from 40
to 10,000 feet, the average being 362 yards. The direction
of the whirling movement of the tornado was invariably from
right to left, or the opposite of the movement of the hands
of a watch, resembling in this respect the vorticose move-
ment of cyclones in the northern hemisphere. The passage
of the tornado cloud is often described as accompanied
with remarkable noises, which observers variously charac-
terize as terrible, deafening, a terrific crash, the roar of a
thousand trains of cars, or the uproarious din of innumer-
able pieces of machinery.
The usual position of the gyrating columns of cloud is
vertical ; but occasionally a cur^Tng form or slanting
direction is assumed. It is probable that to these latter
forms many stationary or slowly moving dangerous squalls
are to be referred, which spring up with unexpected
suddenness in lakes and arms of the sea in mountainous
regions.
The dust storm of India, Arabia, and Africa is a well-
marked type of the whirlwind. Previous to the outbreak
of a dust storm the air is unusually calm and sultry, just
as happens in the case of the tornado. The simplest form
of the dust storm is that of a tall aerial column of sand
moving onwards, and drawing into itself, as it whirls round
in its eonrse, dust and other light bodies vrithin the sweep
of the strong air-currents which blow along the surface of
the ground and converge vorticosely round the base of the
column. A form commonly seen is shown in fig. 7, which
represents several dust columns grouped together, each
whii-ling independently round its own axis with incurving
air-currents at the. base, while the whole group of columns
is borne bodily forward, and presents striking aspects as
the forms and relative positions of the columns are changed.
The importance of the observations made on dust storms
as leading to a correct understanding of the Avhirlwind
consists in this that it alfords conclusive evidence that
there is a strong inflow of the
air along the surface of the
ground all round vorticosely
towards the base of the whh-1-
wind, aud that these same in-
flovNTng air-currents afterwards
ascend through the air along
the central axis of the whirl-
mnd, carrying with them the
evidence of their ascent in the
visible solid particles of dust,
sand, and other light objects
they whirl up with them in
their ascending course.
Owiug to the extreme dryness
of the air-currents involved in
the dust storm, the rarefaction
generated by the rapidity of the
gyrations is insufficient to pro-
duce condensation of the aqueous
vapour in the interior of the
column. Quite different, how-
ever, is it with waterspouts and
torng,does, where, in the great
— majorit3' of cases, the air near
the surface before being drawn
into the ascending cortex is of
a high temperature and near the point of saturation
From the extreme rarefaction to which these air-currents
are subjected, owing to their sudden ascent in a rapidly
gyrating column, excessive condensation follows, vrith an
aqueous precipitation at times so astonishing that it can
only be fittingly _ _ _
described as
aerial torrent of
solid water, or an
aerial avalanche
of hail and ice
Certain tracts
of the ocean in
eluded within
what may
called permanent
anticyclones, or
where atmo-
spheric pressure
is higher than all
round, are char
acterized by an
absence or com
parative absence
of rain. These
regions are also
remarkable for
clear skies and
strong sun heat.
§4^^: vsoaT'
Fia 7. — Dust Storm.
Similarly small anticyelonic areas occur-
ring between or in the vicinity of cyclones are characterized
by dry air and clear skies, and it is under these conditions
that the strongest sun heat is felt. When, as repeated!/
132
METEOKOLOGY
tSAIL.
happens in the warmer months of the year, anticyclones
remain practically stationary for some time, the lowermost
strata of the air become abnormally heated, — thus bringing
about a vertical disturbance of the equilibrium of the atmo-
sphere out of which whirlwinds originate. It is under these
conditions that white squalls or fair-weather whirlwinds
occur, the originating cause of this special form being the
great dryness of the air due to its place in the anticyclone,
and the abnormally rapid diminution of temperature and
humidity with height owing to the strong insolation through
the clear dry atmosphere. The clouds accompanying the
white squalls are at a great height, but the commotion and
boiling of the sea under them and following them as they
drift onwards show that the squalls are true whirlwinds,
the vapour column of the waterspout not being formed
solely on account of the extreme dryness of the air which
ascends the columns. The white squall accompanies fine
■weather, and its appearance is sudden, its duration brief,
and its destructive power at times so dreadful tliat it has
been known to strip a ship of every sail and mast in a few
seconds, and leave it rolling a helpless log amidst the
tremendous sea which follows it. In sailing through such
regions a close lookout should be ma.de, particularly when
the weather looks singularly fine, the skies beautifully
clear, the air calm or nearly so, and the temperature and
moisture of the air on board the vessel noticeably high.
Diurnal Period of Hail. — The hail here referred to is
round, hard, and compact, and in the form of clear or
granular ice, the hailstones sometimes being found when
broken across to be composed of alternate layers of these
two states of ice. The following figures show the number
of times it has occui'red during the different hours of the
day at Coimbra during the last six years : —
Midt to 2 A.M. 0
8 A.M. to 10 A.M. 3
4 p.m. to 6 P.M
2 A.M. „ 4 „ 1
10 „ „ Noon 20
8 .1 .. 8 „
« „ „ 6 „ 2
Noon „ 2 P.M. IB
8 „ „ 10 „
« .. ., 8 „ 1
2 P.M.,, 4 „ 13
10 „ „ Midt.
A diurnal period is thus well-marked at Coimbra, where
forty-eight out of the fifty-nine ca.ses have occurred from
10 A.M. to 4 P.M. This period is essentially the same as
those calculated for a large number of places in representa-
tive climates, care having been taken to limit the inquiry
to the particular hail described above. The important
point to be noticed in the diurnal period of hail is that the
time of maximum is about two hours earlier than the
maximum period of thunderstorms. The maximum period
for the thunderstorm is when the ascending current frpm
the heated land is at its greatest force for the day ; but
the maximum period for hail is some time before the
ascending current has fully established itself, or at that
time of the day when the vertical disturbance of the
atmosphere is greatest, — in other words, when atmospheric
temperature and Vapour fall with height at a much greater
rate than the normal In the higher latitudes hail falls
aJmost exclusively during the warmer months of the year.
In regions where the summer cKmate is practically rainless
no hail falls ; and where the rainfall is small and at distant
intervals few cases of haU occur. Thus at Coimbra, where
little rain falls in summer, hail was recorded as having
fallen only once in the six years during the four dry hot
months from June to September.
All haU is probably connected immediately with whirl-
winds, more or less developed ; and it is whm the b^il-
storm is one of the phenomena attendant on the tornado or
on a great thunderstorm that it assumes its most destruc-
tive form. The theory of the formation of hail has been
stated by Fcrrel in his Mtteoroloyical Researches for the Use
of the Coast Pilot, part ii. p. 85. The vapour carried aloft
by the gyrations of the tornado is below a certain height
condensed into cloud and rain, but above that height into
snow. Let tne raindrops formed below be carried up into
the snow region by the powerful ascending currents of the
tornado and be kept suspended there a little while, and they
become frozen into hail. If now these be thrown quite
outside the gyrations of the tornado, they fall to the earth
as a shower of compact homogeneous hailstones of clear
ice of cfrdinary size. If, however, they are caught in the
descent and carried in toward the vortex by the inflowing
currents on all sides, they are again rapidly carried aloft
into the freezing region. A number of such revolutions
of ascent and descent may be made before they fall to the
earth. While high up in the snow region, the hailstones
receive a coating of snow ; but, while traversing the region
lower down where rain yet unfrozen is carried up, they
receive a coating of solid ice. Thus alternate coatings of
snow and ice are received, and the number of each sort
indicates the number of revolutions described before the
hailstones fell to the ground. When the nucleus is com-
posed of compact snow, as is generally the case, the
hailstone had its origin high up in the snow region as a
small ball of snow, or soft haU {Gravpel in German and
gresU in French) ; but when it is composed of clear ice
throughout it was formed in the rain region, carried up
into the snow region and there frozen, and immediately
aftervrards fell to the ground.
Monthly, Annxfal, and Ikkegttlakly EECtrBRiNa
Pkenombka.
The Temperature of the Sea. — Figs. 8 and 9, represent-
ing the distribution of the temperature of the surface
water of the ocean for the two extreme months February
and August, are reproduced chiefly from The Wind ctnd
Current Charts for Pacific, Atlcmtic, and Indian Octant,
published by the British Admiralty in 1872.
In February (fig. 8) the temperature of the surface of the sea falU
to the annual mmimiun over the northern hemisphere, and rises
to the maximum in the southern hemisphere. The course of the
isothermals more closely follows the latitudes in the Paciiie, Ibdian,
and South Atlantic Oceans ; but the divergence from the latitudes
is great and striking over the North Atlantic. The wider and more
open the ocean the more does the distribution of the temperature
approach the normal; and the more confined the ocean Xh^ greater
is the divergence from the normal. The key to the aiiomalAoa
distribution of the temperature of the ocean is fiirnishi-d hy the
charts of the distribution of atmospheric pressure and the prevailing
winds of the globe. So far as observation has gone itwould appear
that the surface cturents arc practically altogether caused by the
prevailing winds over the respective oceans, subject to such deflexioiu
in their courses as are occasioned by the land.
In the southern hemisphere the currents on the west side of the
Indian Ocean flow southwards along the east coast of Africa, and,
since the currents here pass from lower to higher latitudes, the
temperature along the whole extent of this coast is raised consider-
ably above the normal. On the other liand, since the currents on
the west coast of Africa flow from south to north — in other words,
from liigher to lower latitudes — the ocean currents which impinge
on this coast have a temperature much under the normal. The
winds and currents on the coasts of South America arc pr^*cisely
analogous to tliose of Africa, and the distribution of the tenijierature
of tlie .sea is also similar. The temperature of the ocean on tlic east
coast of that continent is for the same latitudes everywhere higher
than on the west coast. Even in the smaller continent of Australia
the same law holds good.
In the northern hemisphere a ditTcrcnt distribution of the tem-
perature of the sea is seen at this season. In tlie Atlantic the tem-
perature is very much higher on the west of Knrope than on the
east of America. On the feaat of America from u ilmington to
Coaton occur the moat rapid transitions in the mean trmperature of
tlie ocean anywhere on the globe, the tempeniture falling in that
short distance from 70° to 30°, whereas on the eastern side of the
Atlantic these isothermals pass Cape Verd Islands and Spitzbergen
respectively. In the winter montlis the prevailing winds of the
east aid^ of North America are north-westerly, wliilst in tlie central
and eastern portion of the Atlantic they are south-westerly, Ihua
pouring along the ea-^t coast of America the icy currents of the
Arctic regions, but over the central Atlantic and along the western
shores of Europe the irerm water* of southern cluiutea. Tha
rSMFEBATDEE OP SEA.]
METEOROLOGY
133
eut«rly and «outli-easterly winds of Scandinavia in ivinter lower
the isothennals along these coasts. A strikiDg feature of the winter
ijothcrmils of the Atlantic is the singularly high temperature along
the centre stretching from Spitzbergen towards the south-west and
extending in a modified degree as far south as the West Indies. In
the Pacific this feature of the mid-ocean temperature is much less
pronoonced, and the excess of tempcratnre on the west of America
over what occnrs in the same latitudes of eastern Asia is not so
great as the diflerenco observable between the two sides of the
Atlantic.
The highest mean temper.iturc in February (85°) occnrs in iiu
Indian Ocean to the south-west of Sumatra, and there is a patch the
temperature of which is 84* to the north of Madagascar. The
highest means in the Atlantic are 82° in the north-east angle of the
Gmf of Guinea, and 81° off the north-east coast of Brazil In the
Pacific the highest are 83° to the north of the Hji Islands and 81°
near the MarSiall Islands.
Fio. 8. — Isothennals of the Surface of the Sea for February.
In August (%. 9) the southern half of the Ked Sea shows a mean
temperature of 90°, being the highest mean recorded for the ocean
anywhere at any season. Patches showing a summer mean of 85*
occur in the Chinese Sea to the east of Tonquin, in the Bay of
Bengal to the east of southern India, about Socotra, and to the
west of Central America. But the most extensive regions of high
temperature are in the west of the Pacific between long. 165°
E. and the Philippines northward nearly to Japan and south-
waid to Kew Guinea, and the Gulf of Mexico and the adjoining
part of the Atlantic as far east as long. 57° W. A patch of
nmaxkably low temperature occurs in the Pacific a little to the
Tig. 9. — Isothennals of the Surface of the Sea for August.
west of Galapagos, where the mean is only 70°, being 10° lower than
what occurs anj-where else near the equator at this season.
The influence of currents is strongly expressed in the temperature
of all the oceans. In the south of Asia the monsoons are S.W.,
8., and S.E. Under the impulse of these monsoonal winds an
extensive surface drift of the waters of the equatorial regions is
134
METEOROLOGY
[TElIPEEA.rUP.E.
carried northwards towards soutliern Asia, aiij consequently very
high temperatures characterize these ocas in summer. It is iustruc-
tive to note the efl'ect on the temiierature of the sea resulting from
the region of high atmospheric pressure in the Norlh Atlantic at
this season. Out of this anticyclouic region the winds hlow in all
directions, giving rise to surface currents Ilowing in the same direc-
tions. Thus to the west of Africa the winds and currents are from
north to south ; and hence the temperature of this part of the ocean
13 abnormally reduced. On the other hand, on the west side of this
high pressure area, the prevailing winds and currents are from south
to north, and it will be seen that the temperature of the whole of
the region swept by the southerly winds is abnormally raised. On
the north side of the area, the winds and currents are westerly as
far as about long. 35° W. , and over that space the isothermals
follow the parallels of latitude. Farther to eastward and northward
the prevailing winds become south-westerly, thus propelling north-
wards along the western shores of Europe, by oceanic surface drifts,
the warmer waters of southern latitudes. Meanwhile the currents of
cold water and ice drifts from the Arctic regions keep the tempera-
ture off America to the north of Newfoundland at a figure con-
siderably lower than is observed in any other region in the same
latitudes. In August similar relations exist as in January between
the east and west coasts respectively of South Africa, South
America, and Australia, all of which are readily explained by the
charts of mean atmospheric pressure and the resulting prevalent
winds.
One of the most striking facts of ocean temperature is that the
temperature of the Southern Ocean from about 50" to 60" S. lat.
is practically the same in January and August, a circumstance due
chiefly to the magnificent icebergs of that ocean.
The Taiiperature of the Land. — In regions where the
rainfall is distributed through all the months of the year,
and where snow covers the ground for only a small part
of the year, the mean temperature of the soil nearly equals
that of the air. But when the year is divided into wet
and dry seasons, and when snow Ues during a considerable
portion of the year, the mean annual temperature of the
soil may be above or below that of the air. The greatest
difference between the temperature of the soil and that of
the air occurs where the sm^ace of the ground is covered
during several months with snow. Snow is a bad con-
ductor of heat, and thus obstructs the free propagation of
the cold produced by radiation downwards into the soil,
and the escape of heat from the soil into the air. In this
way, over a considerable portion of the Russian empire,
the temperature of the soil is considerably in excess of that
of the air. Thu.s at a place 120 miles south of Archangel
the temperature of the soil is 10° higher than that of the
air; and at Semipalatinsk it is 9° higher.
The daily changes of temperature only affect the soil to
depths of about 4 feet. The precise depth varies with
the degree of the svm-heat and with the nature of the soil.
Similarly the heat of summer and the cold of winter give
rise to a larger annual wave of heat propagated downwards,
the amplitude of which diminishes with the depth till it
ceases to be perceptible. Principal Forbes showed from
observations on the Calton Hill, Edinburgh, that the annual
variation is not appreciable lower than 40 feet below the
surface, and that under 25 feet the change of temperature
through the year is small. The depth at which the annual
variation ceases, or where the temperature remains constant,
is a variable depending on the conductivity and specific
heat of the soil or rock, but particularly on the difference
between the summer and winter temperatures. The rate
at which the annual wave of temperature is propagated
downwards is so slow that at Edinburgh, at a depth of 21
feet, the highest annual temperatvu-e does not occur till
January 4, and the lowest till about July 13, thus revers-
ing the seasons at this depth. ' At Greenwich, at a depth
of 25 1 feet, these phases of the annual temperature occur
on November 30 and June 1.
Professor Everett in the Report of the British Association for 1879
ha-i summarized the results of the observations of underground t<!m-
peraturo. The temperature of the surface of the ground is not
sensibly influenced by the flow of heat from below upwards, but is
determined by atmospheric and astronomical'conditions. The tem-
perature gradient is defined as the rate of increase of the temperature
downwards, and it may be taken as averaging one degree Fahrenheit
for every 50 or 60 feet, the exact rate in particular cases being very
variable. Thus the temperatui-o graditnt of the soil is a>>oul five
times steeper than the temperature »,radient of the air. The
temperature gradient is steepest beneath gorges and least steep
beneath ridges ; and hence the underground annual isothennals are
flatter than the uneven surfaces above them. This is the case even
ivith the uppennost isothermal of the soil, and the flattening
increases as we pass downwards until at a considerable depth they
become horizontal Where the surface of the ground and the iso-
thermal surfaces beneath it are horizontal, the How of heat is verti-
cal, and the same quantity of heat flows across all sections whicB
lie in the same vertical. In this case the flow across a horizontal
area of unit size is equal to the product of the temperature gradhint
by the conductivity, if the latter term be used in an extended sense,
so that it includes convection by the percolation of water, as well
as conduction proper ; and hence, in comparing different strata in
the same vertical, the gradient varies in the inverse ratio of the
conductivity.
Since the efl'ects of the cold generated by nocturnal radiation
mostly accumulate on the surface of the earth, but the eiTects of
solar radiation are spread to some height by ascending currents from
the heated ground, it might be expected that the annual tempera-
ture of the surface layer of the soil would be lower than that of the
air resting over them. Observations prove that such is the case.
Springs which have their eoiuces at greater depths than that to
which the annual variation penetrates have a constant temperutnre
throughout the year, and if they do come from a depth considerably
greater than this they may be regarded as giving a very close
approximation to the mean annual temperature of the place. The
temperature of cellars is also very Dear the mean annual temperature
of tlie locality ; at any rate this t.;mperatnre may be secured for
cellars anywhere.
Distribution of Temperature in the Atmosphere. — Of the
larger problems of meteorology, the distribution of tempera-
ture in the atmosphere over the land surfaces of the globe
was the first that received an approximate solution (by
Humboldt). But as regards the ocean, which comprisea
three-foMths of the garth's surface, the question of the
monthly and annual distribution of temperature in the
atmosphere over it can scarcely yet be said to have been
seriously looked at. The isothermals of the temperature
of the atmosphere which cross the oceans continue still to
bo drawn essentially from observations made on the islands
and along the coasts of these oceans. The first step
towards the solution of this vital problem in climatology
and other branches of meteorology is the construction of
charts of mean montlily temperature of the surface water
of the sea over all parts of the ocean from which observa^
tions for the purpose are avadable. In prosecuting this
line of inqidry, excellent work has been dona by the
Meteorological Office as regards parts of the Atlantic
between the tropics and the ocean to the south of Africa,
and ako by the Dutch, French, and German meteorologists.
With such charts it would not be difficult, by a careful
comparison during the same intervals of time between the
temperature of the surface of the sea and that of the air
resting over it, to construct monthly charts of the tempera-
ture of the atmosphere over the oceans of the globe.
In this connexion the whole of the ohser^-ations of the tempera-
tures of the air and »ea made on board the "Challenger " have been
examined, an<l sorted into one hundred and seventy-four groupa
according to geographical position, and the diflerenees entered on a
chart of the route of the expedition. In the Southern Ocean between
latitudes 45° and 60' the temperature of the sea was lower than
that of tile air, the mean diiference being 1°*4. The temperature
of the air is hfro higher owiug to the prevailing "W.N.W. win-la,
and that of the sea lower owing to the numerous icebergs. To
south of lat. 60° S. the sea was nearly 2°"0 warmer than the air,
the result in this case being due to the open sea, which keeps up a
higher surface temperature, and to an increased jirevalcnoe in these
higher latitudes of southerly (rinds, thus lowering the temperature
of the air.
The period during which the temperature of the sea exceeded
that of the air was from June 1874 to March 18"6, or during that
part of the cruise from Sydney to Kew Zealand, and through the
East India Islands to Ilong Kong and thence to the Admiralty
Islands. During the whole of this time, except when passing the
north of Austrili>, the sea waa much warmer than the air, th«
TSHPEBATUBE.]
METEOROLOGY
135
ge-crJ excess being from 2° to 3', rising even near Tongatabu to
upwards >f i°. The climate of the southern part of this extensive
region at the reasons ■■isited has a large rainfall, sinch clond, and
consequently a comparadreij jmiH evaporation and sunshine. In
June, when the "Challenger" passed the north of Australia, the
climate was very dry, the sunsnine strong, and the evaporation
large, and there the sea was slightly colder than the air. In the
Atmntic between lat. 20° N. and 20° S. the sea was everywhere
warmer, the mean excess being about a degree ; and in the Pacific
ietwcen lat. 30° N. and 30° S. the sea was also warmer, the mean
excess being a degree and a half.
On the other hand, in the Atlantic from lat. 40° to 20° N. the
9ea was, on the mean, half a degree colder than the air. This region
ia remarkable for the high pressure which oveiapreads it, for the
winds and currents which now out in all directions, for its clear
skies, strong sunsbine, and consequently Lirge evaporation, by which
the temperature of the surface of the sea ia lowered, and that of
the air resting on it, being open to the heating iuduenca of the sun,
is raised. Similarly in the North PaciBc from lat. 40° to 30° th«
temperature of the surface of the sea was half a degree lower than
that of the air.
These remarks apply ouly to the observations made stjictly ou
the open sea. Near land very great differences were observed
which varied with season. Thus at Hong Kong during the latter
half of November 1874 the sea was 3° 7 warmer than tile air, the
low temperature of the air at this season being caused by the lower
temperature of the land and the northerly winds which then prev.ii! ;
on the other hand, at Valparaiso in November and December of tlw
following year the sea was 5* 8 colder thau the air during the thrc;
weeks the "Challenger" was there, the diflerence being due to the
cold oceanic current which sweeps northwards past that coast, and
the rapid increase in the temperature of the air at that titne of the
year. These results will help us in gaining some knowledge of the
temperature of the air over the oceans of the globe in February and
August, taken in connexion with a careful examination of the lea
temperature of these months represented in figs. 8 and 9.
Fio. 10. — January Isothermals of the Surface of the Globe.
The distribution of tempemture over the surface of the
globe is sho^vn by figs. 10 and 11, which represent the
temperature of the two extreme months January and July
for the eleven years 1870 to 1880. The region of highest
temperature, which may be regarded as comprised between
the north and south isothermak of S0°, forms an irregularly
shaped zone, IjTng in tropical and partly in subtropical
countries. On each side of this warm zone the tempera-
ture diminishes towards the poles, and the lines showing
snccessively the gradual lowering of the temperature are,
roughly speaking, arranged parallel to the equator, thus
showing in an unmistakable manner the predominating
influence of the sun as the source of terrestrial heat. While
this decrease of temperature corresponds in a general way
to what may be called the solar climate, there are great
deviations brought about by disturbing causes.
Among these disturbing causes the unequal distribution
of land and water holds a prominent place. In January
the earth presents to the perpendicular rays of the sun the
most uniform eiu^ace, or the largest water surface, and
in July the most diversified surface, or the greatest extent
of land. Hence the zone of the earth's surface comprised
between the isothermaU of 80° is less irregular, and also
.spreads over an area more restricted, in January than in
July. In J'lly the areas enclosed by the isothermals of
£0° and 90° are much larger in the Old World than
13 the Nsw, it being the former which presents the krger
land surface to the perpendicular rays of the sun ; and in
January, the summer of the southern hemisphere, the moat
extensive area of high temperature occurs in Africa and
the least in Australia, the high-temperature area of South
America being intermediate. In contrast to this tLe belt
of temperature exceeding 80° is of least breadth where it
crosses the Pacific and Atlantic Oceans, the absolute
minimum breadth being in July in the Pacific, the largest
ocean, where the disturbing influence of the land is least.
During the cold months of the year, when the sun's heat
is least and the effects of terrestrial radiation attain the
maximum, the greatest cold is over the largest land
surfaces which slant most to the sun. Thus the lowest
mean temperature that occurs anywhere or at any season
on the globe is -55°-8 at Werchojansk (lat. 67° 34' N.,
long. 133° 51' E.) in north-eastern Siberia. In Arctic
America the lowest isothermal is — 40°-0. During the
winter the ocean everywhere maintains a higher tem-
perature in all regions open to its influence, as i.5 seen, not
only in the higher latitudes to which the isothermals push
their way as they cross the Atlantic and Pacific, but also
in their irregidar courses over and near the Jlediterranean,
Black, Caspian, and Baltic Seas, Hudson's Bay, the mouth
of the St Lawrence, the American lakes, and all other lar.ge
sheets of salt and fresh water. The disturbing influence
of sheets of water on the temperature in all seasons is very
strikingly shown when the isothermals are.drawn for every
136
METEOROLOGY
rXEMPEKATUEB.
degree, these marking out the prominent features of local
climates, a knowledge of which is of so great importance to
the agriculturist, the horticulturist, and the invalid. Figs.
12 and 13 represent charts of temperature of this descrip-
tion for the British Islands for 1870-1880 from the
Jour, of ^cot. Meteor. Soc, vol vi. In the wijeter of the
Fio. 11. — July Isothermal of the Surface of the Globe.
BOUthcm hemisphere the depressing influence of the land
on the temperature is bat sHghtly felt, owing to the small
east of AustraUa and in the basin of the La Plata, a lower
temperature prevails in the interior.
Another prominent disturbing cause operating on the
FiQ. 12.— Mean Tempc-ruturc of the British Islamls in January.
extent of the land surfaces and the comparatively low
latitudes to whigh they extend southwaids. In the south-
Fio. 13. — Mean Temperature of the British Islands in July.
mean temperature is to be found in the seasonal areas of
low and high mean pressure in their connexion with the pre-
vailing winds. Of these the most marked is the system of
TEWPEEATCrEE.J
METEOROLOGY
137
low pressure about Iceland during the tuinter months (see
fig. 14). Since this region of low pressure gives to western
Europe itB prevailing sotith-west and south winds, and to
North America its north-west winds in winter, it is plain
that the temperature of western Europe is thereby
abnormally raised by the simple fact of its prevailing
winds coming from the ocean and from lower latitudes,
and that the temperature of North America is abnormally
lowered by its prevailing winds coming from the Arctic
regions and from land. The opposite action of these two
winds, which are part and parcel of the same atmospheric
disturbance about Iceland, is shovni from the fact that,
while the mean temperature of the south coast of Hudson's
Eay in January is — 20°, in the same latitude in the
Atlantic to the west of Scotland it is aa high as 44°, or
64° higher. A similar though less striking result accom-
panies the low-pressure area in the north of the Pacific in
winter.
Another area of low mean pressure which powerfvilly
affects the temperature is the low barometer which over-
spreads the interior of Asia during the summer months
(see fig. 17). Since from this disposition of the pressure the
prevailing winds of Europe and western Asia are north-
west and west, and over eastern Asia south-east and east,
it follows that the temperature is abnormally raised on the
eastern side and depressed on the western side of the con-
tinent by the direction from which they severally receive
their prevailing winds. This is well shown by the course
of the summer isothermals of 80°, 70°, 60°, and 50° across
the Old Continent.
Since the strongest insolation occurs where the air is
<lriest, the hottest summer climates are met with in those
tropical and subtropical regions where no rain falls. The
most extensive of the rainless regions during the summer
months is perhaps that which extends from the Punjab
westwards through Persia, Arabia, and North Africa to
Spain. This is the region where the hottest climates of
the globe arc to be encountered. Similarly no rain falls at
this time of the year in lower California and the States
adjoining, and this feature of the climate, taken in con-
Bexion with the relatively low temperature of the coast due
to the winds and ocean currents from the north which
sweep past it, results in sharp contrasts of temperature
within short distances such as have no parallel in any other
climate.
Of the areas of seasonal high mean pressure, the high
barometer of Central Asia in ^vinter stands out in character-
istic prominence (see fig. 14). Now, since the prevailing
winds which necessarily form a part of this feature are south
and south-west over Russia and western Siberia, the tempera-
ture of these inland regions is considerably higher than
would otherwise be the case. On the other hand, since the
prevailing winds are north-west in eastern Asia, the tempera-
ture of these regions is thereby abnormally depressed. It
is this consideration chiefly which explains how it is that,
while the mean January temperature in latitude 60° and
longitude 120° E. is - 30°, in the same latitude but in
longitude 43° E. the mean 'temperatiu-e is 10°, or 40°
higher, even though both regions are equally continental in
their character.
The high mean pressure in the summer in the Atlantic
between Africa and the United States has with its system
of -ninds the most decided influence in bringing about the
abnormal distribution of the temperature of that and
adjoining regions. Since on its west side the prevailing
winds are necessarily southerly, the temperature . of that
region is abnormally raised, and, on the other hand, since
on its east side the winds are northerly, the temperatuie
of the region is abnormally depressed. The result of these
■t^vo opposite winds is seen in the slanting direction of the
isothermal of 80° across the Atlantic, which slanting
direction is continued far into the interior of North America
for the reasons already stated.
These important bearings of cyclonic and anticyclonic
areas on temperature and climate may be thus summarized.
The temperature is abnormally raised on the east sides of
cyclonic areas, and abnormally depressed on the west sides ;
but, on the other hand, temperature is abnormally raised
on the west sides of anticyclonic areas and depressed on
their east sides. In the southern hemisphere these direc-
tions are reversed.
Another set of influences, powerfully affecting the tem-
perature, come into play where the siu^ace of the land
rises above the sea into elevated plateaus, lofty peaks, or
mountain ranges. Thus it has been observed on Ben
Nevis and other mountains that the mud during the day
in summer exhibits a>n ascensional tendency due to the
circumstance that the temperature of the surface of the
mountain is heated in a much greater degree than the air
strata at the same levels all around it. An ascensional
current consequently rises from the mountain, which is
maintained at a steadily stronger rate than at lower levels,
because the drain from the updraught is easily supplied
from the free surrounding atmosphere. It is the strong
insolation at high elevations in the summer months which
explains the excessively high day-temperatures encountered
in the Rocky Mountains ; and from the same conditions,
viz., the rarity and purity of the atmosphere, by which
terrestrial radiation is but httle checked, come the low
temperatures of the nights of these climates in the same
season. From this cause it follows that the elevated lands
in the interior of continents tend to reduce mean atmo-
spheric pressure in summer to a greater extent than woiUd
otherwise be the case. In winter, on the other hand, the
temperature of elevated regions in the interior of continents
is very much colder than that of the surrounding atmosphere
at the same height.?, because in such regions the air is
exceedingly dry and lare, and consequently radiation to
the cold regions of space but little checked. Hence down
the slopes of these high lands there are poured in all
directions descending currents of very Cold air, which
intensify the rigours of the winters experienced on the low
lands round their base, where accordingly the lowest mean
winter temperatures occui-. These elevated lands thus
materially add to the high atmospheric pressure of the
interior of continents during ihe cold months of the year.
But it is ocean streams and ocean currents which produce
the greatest abnormalities in the distribution of the tempcia-
ture of the air, and a glance at figs. 10 and 11 will show
that it is in the North Atlantic where this cause is most
strikingly seen. The increase thus accruing to the winter
temperature is greatest about the north of Norway. It is
also very great in the British Islands; thus, if no more
heat were received than is due to their position on the globe
in respect of latitude, the mean winter temperature of
Shetland would be 3° and that of London 17°. But
mainly owing to the heat given out by the Gulf Stream
and other warm currents of the Atlantic their mean winter
temperatures are respectively about 39°"5 and 39°, Shetland
being thus benefited 36° '5 and London 22°. The chart of
the ^winter temperature of the British Islands well illustrates
the influence of the surrounding ocean in maintaining a
higher temperature. It will be seen that the south-west
of Ireland is 7° warmer than the east coast of England in
the same latitudes. The strong drift current from near
Behring's Strait southward along the coast of America lias
a powerful influence, particularly in lowering the summer
temperature of that coast, — thus bringing about, in con-
junction with the dry rainless climate of the interior, what
are perhaps the most violently contrasted climates, within
^ SVI. — i8
J35
METEOROLOGY
[aqueous vxpotr*.
aarrow limits, as regards their temperature. The deflexions
of the isothermals near the Baltic, Mediterranean, Black,
and Caspian Seas and the freshwater lakes of America
all point 10 tLo disturbing influence of these sheets of
water on the temperature.
The liei-'lit and direction of mountain ranges is an
important element in deteinuidng climate. If the ranges
are perpendicular to the prevailing winds and of a con-
siderable height, they drain the winds of much of thiir
mo;stiU"e, thus causing to places to leeward colder winters
and hotter summers, by partially removing their protecting
screen of vapour, and e.^qiosing them more completely
to solar and terrestrial ladiation. Of this Norway and
Sweden and the British Islands form excellent illustrations.
It is this that makes the most important distinctions
among climates in regions near each other, as respects both
animal and vegetable Ufe. With regard to the decrease of
temperature with height, very much yet remains to be done
before an ajjproximation to the law of decrease can be
stated. During the five months observations Avere made
on Bon Kevis in the summer of 1881 the difference
between the mean temperature at sea-level adjoining and
at the top of the Ben, diOG feet above the sea, was iri°'7,
■which shows a mean decrease of 1° Fahr. for every 280
feet of elevation. The actual differences from day to day
varied from V'i to 23°'2. As Ben NeA-is forms a peak,
and is in the vnry middle of the strong winds from the
Atlantic, it is highly probable that this rate of decrease is
a close approximation to the true decrease of the tempera-
ture of the air during the svimmer months in that part of
the British Islands. When observations are made on
elevated plateaus of some extent, the rat« of decrease
deduced from the observations will be less than the true
rate in the free atmosphere in summer and grenter in
winter. The rate is thus a variable (juantity, varying with
latitude, situation, dampness or dryness of the air, calm or
windy weather, and particularly with tl)f' reason of the
year. One degiee Fahrenheit tor every SC"'.' i.-- the rat-e of
decrease generally assumed.
Aiiwunt of Aqueous Vapmir. — It is scarcely possible to
overestimate the importance of a knowh^lge of the hori-
Eontal and vertical distribution in the atmosphere of its
aqueous vapour, for it may be truly said that it forms one
of the prime factors in all the larger problems of atmo-
.spheric physics. A first rough approximation to the geo-
graphical distribution of the vapour of the atmosphere was
published by Mohn in 1875 in his G-rund:iige der Meteoro-
Ifffie, p. 84, in which vapour-pressure curves are drawn for
the globe for January and July. These leave much still
to be done, not only in a fiu-ther discussion of observations
already made, but also in improvement of the methods of
observation and in the tables for their reduction. The
chief point of interest in Mohn's vapour curves is their
striking resemblance to the isothermals of the same months,
and they also suggest that this line of inquir)' is yet des-
tined to make large contributions to our knowledge of the
unceasing changes which occur in tlie pressure, temperature,
cloud, rain, and movements of the atmosphere.
Still less is known of the vertical distribution of acjiieous
vapour. It decreases, like temperature, with the height,
and if the staiemeut geuentlly made be at all correct, that
half of the A\holc vapour of the otmosiihere is contained in
the lowest GOOO feet, and that at 20,000 feet higli there is
only about a tenth of what is at the earth's surface, the rate
of decrease with height proceeds at a greatly more rapid rate
than is consistent with the supposition that it forms an
independent vapour atmosphere existing rmder its own
pressure.' The establishment of an increased number of
high-level stations, and a more systematic inquiry than has
yet bteu attempted into the upper ciUTtUvS of the atmo-
sphere, are much needed in the further development of tiiis
branch of meteorolog)'. In carrjTug out the inquiry,
invaluable assistance will be obtained from observations of
the diurnal range of the barometer and from well-devised
methods of obsernng the effects of solar radiation at the
earth's surface.
Amou7ii of Cloud. — In Scotland, which lies completely
within the region swept by the south-westerly winds from
(he Atlantic, and presents a well-defined mountain range
lying across the track of these winds, the clouds have a
distinct annual period. In the west, at places quite open
to these westerly breeze.s, the amounts of cloud in spring,
summer, autumn, and winter are respectively 67, 69, 71,
and 74, and the annual mean 70.' In the east, in such
districts as East and ilid Lothian, which have extensive
ranges of hills between them and the Atiantio, the propor-
tions are 09, C3, 62, and 60, and the annual mean 61.
Thus about a teuth more of the .-^ky is covered with cloud
at the western as compared with the eastern situations, and
the distribution of cloud difrers materially in western and
eastern '-liuiates. In the west winter is the cloudiest
season, but in the east it is summer, and these are respec-
tively the months when most rain falls in the several
climates. Everywhere .spring is the .season when the sky
is cli'iarest. In England, owing to the protection afforded
by Ireland and Wales to the west and the comparative
absence of ranges of hiUs, the amount of cloud is Ic^^s than
in Scotland, and it is more equally distributed over the
country. The minimum amount occurs in spring, and the
maximum in winter and autumn.
Sonio of tlie best illustrations of the seasonal variation in the
distribution of cloud are aflorded by the Old Continent. These
variations are the simple cousequence of the systems of wiai
caused by the high winter and low summer pressures of that conti-
nent. In eastern Siberia the prevailing winds in winter are N.W.
or continental, and in siunmer 3.E, or oceanic; and accoi\]icgly
;it AJan, ^Nci-tchinsk, and F.lagoweshtcbf-iisk the moan amounts
of cloud in these two seasons are 18 and -11. On ttie other hand,
in western Sibeiia and eastern Europe the prevailing winds ia
winter are S. W., or from lower to higher latitudes, and ia
sumniei N.W. , or from higher to lower latitude?. Kazan niay^
taken as fairly representing this extensive region, and there the
amounts oi ;;ioud for the four seasons beginning witii winter
are 71, 48, 44, and 62. As the N.AV. winds of summer rise over
the Ural mountains in their course, condensation of the ax|ueoq#
vapour is increased, and Iience over this region the cloud in winter
and siuumer is nearly the same, the mean amounts at Bogoslovsk,
Ekaterinburg, an! Zlatoust being respecti vely GG and 52. At Tiflis
and Kutais, sita.i'ad on the high ground wliieh lies betwetin the
Black Sea and r.,.- south of the Caspian Sea, the means for winter
and summer arc f3 and 55. On the eastern coast of the Black Sea
the westerly winds of summer are accompanied with the annual
maximum cloud, the winter and summer amounts at Redut-Kale
being 59 and C'.i. In Central Siberia, to which the S.W. winds <rf
^\'inte^ do not extend, and to the nortli of latitude 55°, tlie amount
of cloud is much di'iiinislied, and the cloudiness of summer is nearly
the same as that of winter. ■ ,
In India, in all regions which lie open to the summer monsoon,
the minimum amount of cloud occurs during the winter and
the maximum in summer, — the mean amounts being It) i'.ud 74
at CaUutta, 16 and 56 at Bombay, 48 and 71 at Colombo, and
25 and 90 at Rjingoon. At Trineomalee, on the ea.st cc;ist of
Ceylon, and thus exposed to the rains of the N.E. monsoon
of winter, and largely pi-otccted from the rains of the S.W.
moisoon of summer, tlie amounts of cloud in these seasons .ii-e 52
and 59. At l).irj;iing (0912 feet) and Chakrata (7022 feet high),
both on the llimahiyas, whither the summer monsoon penetrates,
the mean amounts are respectively 53 and 86, and 43 and 73. At
Leh, in K.ashmir, the amounts are 69 and 61, the excess being thus
in winter. lu tlie Punjab and to westwards, or those regions ia
southern Asia to which tlie summer monsoon does not extend, the
cloud in winter is cverj'whero greater than in summer. Thus the
amounts are 24 and 18 at Mooltan, 33 and 25 at Peshawar, 27 and
10 at Jacobabad, and at Quctta, in lialuchistau, 5600 fe. t high, 42
and 14. Similar relations as to cloud obtain in Australia and the
other continents where high pressures rule in the interior dnring
* In this section the amount of cloud is stated in pereeotages of tii«
l.y icvtred with ckud.
JlTMOSrHBRIO PEESSUKE.]
METEOROLOGY
139
the cold months and low pressures daring the warm months of tnc
year. The maximmn cloud occuis~with winds from tho sea and
winds adTancing into the colder regions of higher latitudes, and
the minimum with winds which have traversed an extensive track of
land and winds advancing into the warmer regions of lower lati-
tudes. As the subject, however, is essentially one with rainfall, it
is not necessary to prosecute it further.
The other atmospheric movements on which the amount
of cloud depends are the ascending and descending currents
of the atmosphere, — the ascending currents with clouded
ski'js occurring in the belt of calms and ove: cyclonic areas
and regions, and the descending currents with compara-
tively clear skies over anticyclonic regions. The region
of maximum vapour and densest cloud-screen on the globo
is the equatorial belt of calms between the trades, which
has an annual movement northward and southward with
the sun as already explained. To ascensional movements
b to be ascribed part of the cloudiness of the southern and
eastern sides of the winter cyclonic regions of the North
Atlantic and North Pacific, and of the cyclonic regions of
low summer pressure in the interior of Asia and other
continents. On the other hand the comparatively small
amount of cloud in the anticyclonic regions of the Atlantic
and Pacific Oceans, and in the high-pressure regions of fho
interior of Asia and other continents during the cold months
of the year, is due to the vast down-currents which occupy
the centres of the anticyclones, and which become
relatively drier as they descend owing to the increasing
pressure to vhich the air is subjected.
Distribution of Atmospheric Pressure. — The importance
of a knowledge of the distribution of atmosphsric pres-
sure, or of the mass of the atmosphere, ever the globe
in its varying amounts from month to month is self-
evident. Observations teach us that windu ore simply
the movements of the atmosphere that sot in from where
there is a surplus towards where there is a deficiency of
air ; and observations also teach that isobaric maps (i.e.,
maps showing the relative distribution of mean pressure)
and maps showing the prevailing %vinds are in accordance
with each other. Since prevailing winds to a large extent
determine the temperatme and rainfall of the regions
they traverse, isobaric maps may be considered as furnish-
ing the key to the more important questions of meteoro-
Isobars of the Globe and Prevailing Winds.
logical inquiry. At the time of the first publication of
isobaric maps of the globe in 186S, it was impossible to
do more than present the subject in its broad general
features, owing to the scantiness and quality of the
materials then existing. But since then meteorological
stations have been largely multiplied in all parts of the
civilized world, and the general adoption of the issue of
storm humings has necessitated the use of more accurate
barometers and uniform methods of observing. Since
there is thus now the means of a more exact representation
of this fundamental datum of meteorology, we have
prepared a new set of isobaric maps, shewing the db-tribn-
tion of the earth's atmosphere and the prevailing winds
for January (fig. 14), July (fig. 17), and the year. They
have been constructed from mean values calculated for the
same eleven years (1870-80 inclusive) as the isothermal
maps figs. 10 to 13, pressure of 30 0 inches and upward.^
being represented by solid lines, and of 29'9 inches and
under by dotted lines, while the arrows show the directions
of the prevailing winds at the localities indicated by the
leepective arrow-points.
Mean Aimosphfric Pressure in January (fig. 14). — In this month,
when the influence of the sun on the northern hemisphere jails to
the minimum, the greatest pressures are massed over the continents
of that hemisphere, and the least presstires over the nortbem parts
of the Atlantic and Pacific Oceans, over the Antarctic Ocean and
southern hemisphere generally. In the southei-n hemisphere there
are three patches where pressure rises to 30 inchea, wz., in the
Atlantic bct^'oen South America and Africa, south of the Indian
Ocean, and in the Pacific between Australia and South Amei-ica.
In the northern hemisphere, on the other hand, pressure rises in
Central Aeia to upwards of 30".^ inches, tho mean pressure for
January being ot least 30 '4 inches at Peking. SemipaJatinsk, and
Yenisei, and fully 30 6 inches ai Irkutsk and JTertchinsk, in
the spper basin of the Amur. This is the reeion where the
normal atmospheric prcssu.-e attains to a maximum which is
much higher than is reached in any other region or at any other
time of the year. It will be observed that this region of
highest pressure occupies a position near the centre of the largest
continent. The area of high barometer is continued v.cstward
through Europe, through the horse latitudes .of the Atlantic to
Carolina, snd thence through the United States to California,
whence it crosses the Pacific to Asia. This belt of high pressure
thus completely encircles the globe, broadening as it passes tho
land and contracting as it crosses the ocean. Its greatest breadth
is over Asia and its least over tho Pacific, or where Und and
oce&n attain respectively their mflvimnm dimensions.
METEOROLOGY
140
TV- ™,iw iinrlpr tho avcraco cover the northern portions
,!^rZkF::X"l"c.nl alsf the greater mrt of the Arct.c
rerions In the north of tho Pacifie the "o™-! r^"" [f ^^^
^bont 29 6 inches bet^Yeen Kamoliatka and Afaska. In the
nn? th of the Atlantic, howoyeN a still lower mean pressure obtains
o%° VJar':w^trt':tUtohing from leelandto thesout^^^^
land, the normal at Stykkisholm m the ""th-west ot IceUnd bem
southward by systenas of rnuch h gher F--"-^ 'h ^ ^^^^ ^^^^
found in the Pacific. Ihe result oi uiui B ^
stronaer winds blow northward over the Atlantic ^"'^ J™"*^ V
^:a4^;;Tnf:3rof u:.4"rttnW^^^ maybe referred to as con.
'^Atelt'lVlow pressure passes through the equatorial regions
St U lies qSite north of the equator even ^-J-^^^'^.^
the sun's course is f-t^-^f ^^^ ^and' n 'tiV XT o'cLn the
Tositi n^of m: Une o??ow:t p^efsur: is to the south of the equator
position 0' ^"» ™° . , ^ ^^ a slanting course from near the
fnrtrofS"! car toward! thence'towards the low pres-
Te whiS^iTs at this season in Australia ; its course is then a
Utt e to uoSvaids, and crosses the Pacific to th-^^'-l Xf, "^
' V, ,„ ,;„, Ti-, „.fh ig thus a devious one, being nortu o: tne
when uTdcr the influence of the regions of low pressure ^-h'ch now
wnen '^""'^^^ An^tralia central and southern Africa, and central
Sl'lm" rt In tht tTough of barometric depression nearly
S^^^^Hie trZical storms of the Indian Ocean have their origin.
There are several important modifications of the isobaric linea
as orwfnaUy published.' In 1863 the region of lowest P"^™^° ^°
" ""o"'- J i,„,„;-„t,rr-< in winter was represented as extenaing
Z:iX^ t^'n'oltrcIstW ■ now the La of lowest pressure
is sTen to extend from Iceland south-westward to Greenland. In
Connexion with this point Captain Hoffmeyer discussed the
weathe of th North AftanHc during several winter n>on 1-. »°'i
■weaiuei ui L.I10 TQ7Q wViiVh (^nnrlusivclv showed that tne
published tl"=/;;^"";,^^JY„^i Iceland exertsln the distribution of
aTm::;t£p1e" "owTrlfTnrutiL notbeforcnroperlyrecog.
nS resuuFi ' in the^mean minimum of pressure te.ng localized
S stinc ly to the south-west of Iceland, and that ^.addition to th^
Smum there are two ^"bordinate minima, one in Dav^ Strait,
and the other in the Arctic Ocean midway between Jan Wayen anu
the Lofoten Isles. Tlie investigation further estab ished the fact
!^,t w^en anv narticular one of these three minima plays an
mtrtant part! tUotl^r two either do not appear at all or occupy
aTe a suLrdinate place, and that according as one or other of
fc min ma of pressure predominates so is the character of the
l„!^l,riL7 regards mildness or severity, of the winter of north-
[iTMOSrHHUO
f„™« in the earlier nart of their course is from Tema to
i^erican storms m the earUerimrL eentres of comparatively
the lakes. ^'?,?fv°".'Y„w barometer readings, cross tl,« southern
rd:rh';a:;rsSei:rher:S:r;interpSsureishigherther,
of 30 inches is deflected to the souin ej^i Amkan 'ftiii
the isobars is particuhirly '■flli"^''!^*^^, the noint is of no small
FiQ IS.-Isobars of Europe for January,
ranean and the countries to the north <>? ^^f ^^ wX^'tJ?
«""?:^30° 0 fn:he '"The* 1 tfeHs" ttiaTge/of the two, a^nd m.v
re^^:^\d:d1.s'?hrpVon,ationoftheregi.nofhi^^^^^^^^
characterizes the Atlantic '■^^'^^'Ld within the isobar 30-15
season. The Wgt-P'.o^'"^ "'=^„^e'"^'eni"it covers a prettr
inches is of peculiar interest In the ^^'^"'^"^^^^ J ^J,
broad area, 'but to the north-east it contracts f » JJ ^ j,
between the Bay of B'3cay and th Gul o^ L^^^^ ^^ ^ P ^^^
to north-eastward »«"°S *fJ'X" ,™ ewhat suddenly intor-
its prolongation eas^vard being ^^^^^^ ;,',?„„,! „gion of high
rupted. .-Stsome distanc o the e^t^^a ^^ ^^^ ^^^^^^
pressure is met with, «luc i is Pfope"y 'p„,,,i„ent in the w nler
[hat overspreads the interior of t O'd C',nt.nent in^^^ ^^,^^
months, if ,«-f™.J^;:"'c^:o"|,*vien:a liibach and the upper
LXr^^slopes^of'thfbas'S'of the Danube, Sebastopol, and thence
Zm^ rottrwordtits position occupiesthe intenor of th.3
the naiuc. >■" "'i"'^' . . • ^„ 1 ;. j^. ;n«;tructivo to not« that tua
b«^^-^:;H^HTZ^ks^in^ 'It
does not, however, exactly °'^"="1'\', , " "jjorth Sea. owing
lying between tho M^d.torraneana„dtl.o North Se J,
tfoubt to the circumstance that the ^.rv steep na » ^^
from France to Iceland greatly I"''"' ,',« PJXa the abnonn .
of tho northern half of Franc. I f<^o-th„t^_t ._^^^.^^ ^
high pressure which so f™arkamy cua™ represented.
1 '"S C::^:^'A Pre-ure an, separated from eaoh oth«
PRBSSUEE.]
METEOKOLOCiY
141
by a large area of comparatively low pressure overspreading the
greater portion of the Mediterranean Sea, — marked off in fig. 15 by
the isobar of 30 10 inches, within which pressure is everywhere less
than 30 10 inches. This region includes an area of still lower
pressure within the isobar of 30*05 inches, bounded by Sicily,
Corfu, Athens, and Crete. Hence the singularly low pressure which
characterizes the northern part of the Atlantic at this season has its
analogtic in the south of Europe, which is unquestionably due to
the higher temperature and larger humidity of the climates of
Bouthern Enrofte which they owe to the Mediterranean.
It is dfserving of special notice that, wliile the increase of the
norntal pressure of January from Genoa to Geneva is O'OSl inch,
it is only 0'021 inch from Trieste to Riva, and that to the north
of the Adriatic as far as latitude 50° pressure is considerably lower
than obtains to the west and east of that region. An examination
of the daily weather maps of Europe shows that not unfrequently
the storms of north-western Europe on advancing as far to east-
ward as Denmark seem to connect themselves in some degree with
Mediterranean storms prevailing at the time through a north and
Bouth prolongation of a system of low pressures. The comparative
frequency with which this occurs is probably occasioned by the
general drift to eastward of the atmosphere of Europe, considered as
a whole, taken in connexion with the high mountainous ridge
which bounds the Adriatic on its eastern side, from which it follows
that the air overspreading the deep basin of the Adriatic is often
highly saturated with vapour, and this highly satui-ated air is
drawn northwards through centi^al Europe when north-western
Btonns of Kurope with low barometric depression centres .pass across
Denmark and the Baltic. Thus the low normal pressure to the
north of the Adriatic, separating the two regions of high pressure
to the east and west of it, is in some respects analogous to the
low normal pressure of the Mississippi valley, which separates the
higher normal pressures of the Kocky Mountains and of the south-
eastern of the United States.
The influence of land and water respectively in the cold season of
the year is well sho^vn in fig. 16, which represents for every 0"020
inch the normal pressure over the British Islands in January,
drawn from means calculated for two hundred and ninety-five
stations.^
It is in the winter months that the isobars of the British Islands
crowd most closely together, and in accordance therewith strong
winds are then most prevalent The crowding of the isobars
reaches the maximum iu January, forming what is probably the
steepest niean monthly barometric gradient that occurs at any
season anjTv^here on the globe. The point, however, to which
attention is here drawn is the remarkable influence of St George's
Cliannel and the Irish Sea in diminishing the pressures as thev
cross these seas, and of the land in increasing the pressure, which
t in the curves occupj-ing approximately the central districts
of Great Britain from the Isle of Wight to Cape Wrath. Tlii*
shews on a comparatively small scale Uie influence of the land ''n.
Fig. 16 — Isobars of the British Islands for January,
raising the normal pressure, and of the sea in lowering it, during: the:
Fio. 17. — July Isobars of the Globe and Prevailing Winds.
oold months of the year, just as is seen on the grand scale in central
Siberi* and the north of the Atlantic
' Bee Journal qf Scot. MeUorolcgical SoeiUy, voL^-' pp. 4-21.
Mean Atmospheric Pressure in July {^g. 17).— In this month thfr
physical conditions are the reverse of what obtains in January, tho
effects of the influence of the sim on the temperature and humidity
of the atmosphere rising to the maximum in the northern and fall--
142
METEOKOLOGY
[ATMOSrHERIC
ing to tho minimum in the southern licmiaphere. "With the solar
conditions reversed, a comparison of figs. 14 and 17 shows that the
distributionof atmospheric pressure in July is, considered -in a broad
sense, the reverse of what takes place in January.
In tho southern hemisphere atmospheric pressure during the
winter season is above the general average of 30 inches between
lat. 10° and 40° S. This belt of high pressure encircles the globe,
and embraces four regions where pressure rises considerably above
this general high average. These regions are in South Africa, about
lat. 20°, where it rises to a little above 30 '20 incliey; in Au'^tralia,
wliere it rises on tho Murray river very nearly to 30 "20 inches;
in South America, where In the basin of the La Plata, about lat. 30',
it rises to 30*13 inches ; and in the ocean to westwards, where it
reaches 30 02 inches. The point to be noted with respect to tlie
position of these centres of liigh pressure at this season is that they
occur over surfaces between latitudes 20' and 36°. As comparetl
with January, pressure in July over nearly the whole of this broad
bolt of tho southern hemisphere is about two-tenths of an inch
higher, which is the simple result of season. A comparison of
January and July shows that this largo accession to the pressure of
the southern hemisphere is accompanied by an extraordinary dimi-
nution of pressm-e over the continents of the northern hemisphere.
Now, just as the greatest excess of pressxirc during the winter
of the northern hemisphere occurs in the continent of Asia, so the
greatest diminution ot pressure in the summt-r months takes place
in the same continent. The position, however, of these two extremes
is far from being in the same region or even near each other. In
the Old Contintmt the maximum occurs in tlie valley of the upper
Amur, where, at Nertchinsk, th«i iiovmal pn -sure in January is
about 30 '500 inches ; whereas the lowest normal pressure in July is
29 "412 inchos, and occurs, so far as observation enables us to locate
it, at Jacobabad on the west side of the ba-;iu of the Indus. The
difference of these two normals is 1 "188 inch ; and over no inconsider-
able portion of central Asia the normal pressure of July is an inch
less tlian that of January. In other words, the influence of the sun
in summer as exerted on the temperature and aqueous vapour of the
atibosphere and atmospheric movements resulting therefrom is so
powerful as to remove a thirtieth part of the whole mass of the
air from this extensive region.
The large extension in recent yeara of good meteorological stations
over the Russian and Indian empires enables us to lay down with
much greater precision than formerly thi; lines of pressure. Of tho
changes indicated by the new isobars, the most important jierhaps
is the position of the region of minimum pressure in Asia, which is
now seen to occupy the basin of the Indus, and thence stretches
over a somewhat broad region to westward nearly as far as the head
of the Persian Gulf. The point is of no small importance in atmo-
splieric physics, inasmuch as it places the region of least normal
pressure in July as close geogiaphically to the region where at the
time terrestrial temperature is highest as the region of highest normal
pressure in January is situated with respect to the region where in
that month terrestrial temperature is lowest in Asia.
The July isobars of India are of singular interest, and imply con-
sequences of tho utmost pi'actical advantage to tho empire. From
Cutch southward the normal pressure is everywhere higher, and
considerably so, along the whole of the west than it is in the cast in
the same latitudes, the difference being approximately half a tenth
of an inch. This is represented on the map by the slanting of the
isobars from north-west to south-east as they cross this part of
India ; and it is tp be noted that the cast and west coasts of Ceylon
show the same manner of distribution of the pressure. The conse-
quence of this jieculiarity in the distribution of the pressure is that
the summer monsoon blows more directly from the ocean over
western and southern India than would have been tho case if tho
isobars had lain duo east and west, and thus probably precipitates in
its course a more abundant rainfall over this part of the empire.
But a more important consequence follows from the geographical
distribution of the pressure over the valley of the Ganges. If the
normal pressure there had diminished ia tho .manner it does over
India to the south of the Gangetic valley, the winds would have
been south-westerly and the summer climate practically rainless,
'i'his, however, is not tho case, but tho normal nrcssure diminishes
westwards along the valley of tho Ganges, as tne following mean
July pressures will show :— Calcutta, 29-576 inches ; Patna, 29*535
inches ; Lucknow, 2&-522 inches ; Roorkce, 29-505 inches ; and in
crossing '.westward into the Punjab pressure falls still lower — to
2!) "439 inches at Mooitan and 29'n2 inches at Jacobabad. Indeed
pressure in July is 0*220 inches lower at Jacobabad than at Sibsagar
on the Br.ihmaputra, nearly in the same latitude. It necessarily
follows from this distribution of tha pressure that the summer mon-
soon, which blows northward over tho 15ay of Bengal, is deflected
into an E.O.E. wind which fills the whole valley of the Ganges,
distributing on its way a most generous rainfall over thai magnili-
cent region.
Ihp inlluonce of the land in lowering tho pressure in summer is
well "illustrated by the course of tho isobars over western Siberia
and Russia, where pressuro ia seen to fall relatively lowest along
the middle line of the Old Continent. In this connexion it is
interesting to note tho course of the isobar of 29*90 inches orer
that part of Europe where the breadth of the land is considerably
increased — between tho Baltic and Constantinople. In contradis-
tinction to this tho influence of the Aral, Caspian, anil Black Seas
in maintaining a higher pressure appears in the remarkable pro-
longation eastward of tiic isobars of higher pressure over the region
of these sea.i, being in striking contrast to the lower pressures which
prevail to the north and south.
The lowering of the normal pressure is very decided in the inland
regions of Spain, North Italy, and Scandinavia. The effect iamost
strongly seen in Spain-, tho largest and compactest of these regions.
Thus, while tho normal' pressure diminishes between Lisbon and
Barcelona from 30*086 to 30'048 inches, tho sea-level prcssui-fe at
Ma<lrid falls nearly to 30*000, and the pressure at Sai-agoisa and
Valladolid is nearly as low. This lowering of the pressure over the
interior influences materially its summer climate. As remarkable
an illustration of the principle as can be pointed to anywhere is seen
in the north of Italy ; for, while the nonnal pressure at Moncaiieri
is 29*941 inches, at Genoa on the coast the relatively liigh normal
of 29*992 inclies is maintained, the distance of the two places being
about 40 miles. To the east pressure rises to 29 970 inches at
Venice, and to westward to 30 "023 inches at Geneva. Over Scandi-
navia, along the west coast from the Arctic circle southward, the
normal pressure equals or exceeds 29*80 inches, the variation beinff
comparatively small ; and along the coast from the head of the Gulf
of Bothnia to the south-east of Sweden pressure also exceeds 29*80
inches, and the increase from north to soutli proceeds at a slow rate.
In, however, the strictly inland districts to the north-cast of
Christiania, which lie immediately to the east of the Scandinavian
mountains, and sheltered by tliat lofty range from the winds of the
Atlantic, pressure is considerably lower than, it is along the cist and
west coasts of the peninsula. Owing to this peculiar distribution
of the pressure, tho winds which necessarily result from it give a
much finer summer climate to the south-cast of Norway and to the
strictly inland part of Sweden than would otherwise be tho case.
The remarkable curving northward of the isobar of 29*80 inches
so as to include Lapland within it points probably to the influence
of the White Sea and the wonderful lake system of Lapland in
maintaining a higher summer pressure over that country, by which
tho northerly winds that blow tov/ards the low-pressure region of
Central Asia, to the serious deterioration of the summer climate of
nortliern Siberia, do not extend so far to westward as Lapland.
The distribution of the normal pressure over North America ia
quite analogous tp what prevails over Asia, but, the contint-nt being
less, the diminution of pressure in the interior is also coii'^spond-
ingly less. The highest normal pressure, 30*077 inches, is found in
the south-east in Florida, and the lowest, 29*780 inclics, in Utah, the
difference being thus 0*297 inch. Another region of relatively high
pressure is ia the north-western States and British Columbia to the
north; the maximum, near the mouth of the Colurnbui river,
seaches 30*062 inches, being thus nearly as high as wltat occurs in
Florida. These two regions are merely extensions of important.
high-pressure areas which at this season are highly characteristic
features of the meteorology of the North Pacific and North Ailantic
respectively
Of these two re^ons of high pressure the one overspread ing the
Atlantic between the United States and Africa is the more striking,
being not only tho region where pressure is highest anywhere o«i
the globe durhig the months of June, July, and August, but where
the normal pressure reaches the highest point attained at any season
over the ocean. The highest point reached by the normal pressure
over the land at any season occurs, as has been pointed out, near tho
centre of Asia, or approximately in the middle region of the largest
continuous land surface on the globe during the coldest months of
the year. On t^lo other hantl, the highest pressure over the ocean
occurs during the warmest months of tho year, and not over the
largest water surface, but in the middle regions of tho North A tlantic,
where the breadth is only about half that of the water surface of tho
North Pacific.
From the essential differences between these two sets of pheno-
mena it may be inferred that the extraordinarily high pleasure
which is so marked a feature of. the meteorology of Central Asia
during tho cold months of the year is a direct consequence of the*
lowering of the temperature of tlie land of Asia and of tho atmo*
sphere rcjting on it during the time of the year when the cffecU of
solar radiatio'ri are at the annual minimum, and of terrestrial radia-
tion at tho annual maximum. But tho determination of the place
and time of highest pressure over the ocean must be regarded sa
indirectly brought about. Tho physical conditions undo.* which it
occurs are those :— it happens (1) At tho time of the year when the
earth presents the largest surface of land to the sun, and (2) over
that part of the ocean which ia most comnletcly surroundo<l by these
higlily heated land surfaces. This high summer pressure of the
Atl.anlic has its origin in the upper currents of the atmosphere.
Mean Atmospheric Pressure for Ike Ye.ar.—T\io distribution of
the annual atmospherio prcssui'e may be considered as representiiig
PSBTAILUra VINDS.]
METEOROLOGY
142
the souu of the influences directly and indirectly at work throughout
the year in increasing or diminishiiig the pressure of the atmosphere.
There are two regions of high pressure, the one north and the
other south of the equator, which pass completely round the globe
as broad belts of high pressure. The belt of high pressure in the
southern hemisphere lies nearly parallel to the equator, and is of
nearly uniform breadth throughout ; but the belt north of the
equator has a very iiTegular outline, and shows great differences in
its breadth and its iiiolination to the equator. These irregularities
whoUy depend on the peculiar di-stribution of land and water which
obtains in the northern hemisphere.
These two" zones of high pressure enclose between them the com-
paratively low pressure of the tropics, through the centre of which
runs a narrower belt of still lower pressure, towards which the trade-
winds on either hand blow. Considered in a broad sense, there
are only three regions of low pressure, the equatorial one just
referred to, and oue round each pole bounded by or contained
within the zones of high pressure just described. The most
remarkable of these, so far as it is kno^vn, is the region of low
pressure about the south pole, which remains low throughout the
year, playing the principal rdle in the i\'ind'systems of the Antarctic
zone, in its heavy snowfall and rainfall, and in the enormous ice-
bergs which form so striking a feature of the water of the Southern
Ocean.
The depression around the north pole contains within its area two
distinct centres of still lower pressure, the one filling the northern
part of the Atlantic and the otlier that of the Pacific. Of these two
the low-pressm-o area round Iceland is the deeper, and is probably
occasioned by the steeper barometric gradients and stronger winds
which prevail over the North Atlantic. The broad equatorial zone
of low pressure also contains two distinct regions characterized by
fitill lower pressures. The larger of the two stretches across
southern Asia from Assam to the head of the Persian Gulf, and is
entirely due to the very low pressures which form so marked a feature
in the summer meteorology of that part of Asia. The regions of
the middle Indus and upper Ganges occupy the centre of this low-
pressure area, where normal pressure falls short of 29 '80 inches.
The second area of lowest equatorial pressure is in the centre of
Africa.
It may be' here pointed out that the whole of these areas of low
mean annual pressure possess the common characteristic of an
excesvive amount of moisture in the atmosphere. The Arctic and
Antarctic zones of low preasure, and the equatorial low-pressure zone
generally, may be regarded as all but wholly occasioned by the com-
paratively large amount of vapour in their atmosphere. As regards
the region of low pressure of southern Asia in summer, it is
remarkable that, while the eastern half which overspreads the valley
of the Ganges is characterized by a moist atmosphere and large
Tainfall, the western half of it is singolarly dry and practically rain-
less, and that the central portion of this remarkable depression
occupies a region where at the time the climate is one of the driest
and hottest anywhere to be found on the globe. Hence, while the
vapour is the more important of the disturbing iijfluences at work
in the atmosphere, the temperature also plays no inconspicuous part
<lirectly in destroying atmospheric equuibriura, from which result
winds, storms, and many oilier atmospheric changes.
The Prevailing Winds of the Globe. — If atmospheric
pressors were equal in all parts of the earth we should
have the physical conditions of a stagnant atmosphere.
Such, however, is not the case. Let there be produced a
concentration of aqueous vapour over a particular region,
or let one region show a higher temperature than what
prevails around it, thea from the different densities,
and consequently different pressittes thereby produced,
the equilibrium of the atmosphere is destroyed, and, as
might be expected from the laws of aerial fliiids, move-
ments of the air, or winds, set in to restore the equili-
brium. Now every one of the isobaric maps we have
given, as well as every isobaric map which has been made
from recorded observations, indicates very considerable
disturbance of the equilibrium at the surface of the earth.
All observation shows that the prevailing winds of any
region at any season of the year are simply the expression
of the atmospheric movements which result from the dis-
turbance of the equilibrium of the atmosphere indicated by
the isobaric maps for tliat season and region.
All winds maybe regarded as caused directly by differences
of atmospheric pressure, just as the flow of rivers is caused
by differences of level, the motion of the air and the motion
of the water being both referable to gravitation. The wind
blows from a r*;^ou of higher towards a region of lower-
pressure, — in other words from where there is a stirplus to
where there is a deficiency of air ; and this taJkes place
whether the differences of prtssuie be measoiable by the
barometer, as is generally the case, or not readily mea.sur-
able, as in the case of sea breezes, squalls, and sadden gusts
of wind which are of short duration.
So far as is known, differences of atmospheric pressure,
and consequently all winds, originate in changes occurring
either in the temperature or the humidity of the air over
restricted regions. Thus, if two regions contiguous to each
other come to be of imequal temperature, the air of the
warmer region, being specifically lighter, will ascend, and
the heavier air of the colder region will flow in below to
take its place. Of this class of winds the sea and land
breezes are the best examples. Again, if the air of one
region comes to be more highly charged with aqueous
vapour than the air of surrounding regions, the air of the
more humid region being lighter will ascend, while tha
heavier air of the drier regions will flow in below and
take its place. SLuce part of the vapour will be condensed
into cloud or rain as it ascends, heat is thereby di.<;engaged,
and the enuilibrium still further disturbed. In this way
c' ;inate gales, storms, tempests, hurricanes, and all the
more violent commotions of the atmosphere, except some
of the forms of the whirlwind, such as dust storms, in the
production of which very great differences of temperature
are more immediately and exclusively concerned.
The Trade- TFinds. — From fig. 14, giving the isobarics
for January, it is seen that atmospheric pressure in the
Atlantic ia lower near the equator than it is to north
and south of it; and the arrows indicate that to the nortli
of the tract of lowest presstire N.E. winds prevail and
to the south of it S.E. winds. These are the well-
known N.E. and S.E. trade-winds, which thus blow from
regions of high pressure towa-rds the tract of lower pressure
situated midway between them. The trade-winds do not
blow directly to where the lowest pressure is, but in a slant-
ing direction at an angle of about half a degree. The devia-
tion from the direct course is due to the influence of the
rotation of the earth on its axis from west to east, — an
influence to which all winds and all currents of the ocean
are subject.
In virtue of this rotation, objects on the earth's surface
at the equator are carried round towards the east at the
rate of about 17 miles a minute. On receding from the
equator, however, this rate of velocity is being continually
diminished, so that at 60° N. lat. it is only about 8J miles
a minute, ai)d at the poles nothing. From this it follows
that a wind blowing along the earth's surface in the direc-
tion of the equator is constantly arriving at places which
have a greater eastward velocity than itself. As the wind
thus lags behind, these places come up, as it were, against
it, the result being an east wind. Since, therefore, the
wind north of the equator is under the influence of two
forces — one, the low pressure near the equator, diawing
it southwards, and the other, the rotation of the earth,
deflecting it eastwards^it w ill, by the law of the composi-
tion of forces, take an intermediate direction, and blow from
north-east. For the same reason, south of the equator the
south is deflected into a south-east wind.
In the Atlantic the north trades prevail between
latitudes 7° and 30° N., and the south trades between lati-
tudes 3° N. and 2.'5° R. These limits are not stationary,
but follow the sun, being farthest to. the south in February
and to the north in August. The tract of low pressure
between these wind systems is named the region of calms,
owing to the calm weather which often prevails there, and
it is also characterized by the frequent occmrence of heavy
rains. This region of calms varies its position with that
of the sun. reaching its most northern limit, lat 11* N.,
144
METEOROLOGY
[PEKVAILINO WISD3,
in August, and its most southern, lat. V N., in February.
Its breadth varies from 3° to 8°, and it lies generally
parallel to the equator. It is to be noted that, in the
Atlantic, the region of calms is at all seasons north of the
equator.
North and south trades also prevail in the Pacific Ocean,
separated by a region of calms, which would appear, how-
ever, to be of less breadth and to be less clearly defined
than ig the region of calms in the Atlantic. In the eastern
portion of the Pacific the region of calms lies at all seasons
to the north of the equator, but in the western division it
is considerably south of the equator during the summer
months of the southern hemi."?phere, this southerly position
being in all likelihood occasioned by the extraordinarily high
pressure in Asia in its relations to the low pressure in the
interior of Australia at this season. During the summer
months of the northern hemisphere the region of cahns
wholly disappears from the Indian Ocean and from the
western part of the Pacific Ocean, there being then an
unbroken diminishing pressure from the latitude of
Mauritius and Central Australia northwards as far as the
low pressure of Central Atia.
Regions of light and variable winds and calms occur at
the higher limits of the north and south trades. Except in
the Pacific, where, owing to the greater breadth of that
ocean, they spread over a considerable extent, these regions
appear but in circumscribed patches, such as characteri2e
the meteorology of the North and South Atlantic about
latitudes 26° to 36°. Of these regions of calms the most
important is that marked off by the high pressure in the
North Atlantic, between the United States and Africa.
This is the region of the Sargasso Sea, where the weather
is characterized by calms and variable winds, and the ocean
by its comparatively stiU waters. These are known to
seamen as the " horse latitudes," and are essentially
different from the equatorial region of calms. The latter,
as has been stated, is the region of low pressure at the
meeting of the north and south trades, where the climate
is distinguished for its general sunlessuess and heavy
rainfall. ~ On the other hand, the calm regions in the
Atlantic and Pacific Oceans about the tropics have an
atmospheric pressure abnormally high, clear skies, and
the weather generally sirnny and bright, with occasional
sqnaUs.
Numerous observations made in all parts of the globe
establish the fact that, while the sxirface winds within the
tropics are directed towards the equatorial region of cahns
in such a manner that the general intertropical movements
of the atmosphere or prevaihng winds are easterly, the
prevailing winds of the north and south temperate zones
are westerly. The westing of these great aerial currents
is due to the same cause that gives easting to the trade-
winds, viz., the rotation of the earth round its axis. For,
as an aerial current advances into higher latitudes, it is
constantly arriving at regions having a less rotatory velocity
than itself ; it thus outstrips them and leaves them behind ;
in other words, it blows over these places as a westerly
wind.
While, however, the general prevalence of westerly winds
has been established over the extratropical regions of
Europe, Asia, Africa, America, and Australia, the direc-
tions which in different seasons and at different places are
actually found to prevail often differ very widely from
west. An examination of the winds at one hundred and
fifteen places pretty well distributed over the northern
hemisphere reveals the iastructive' fact that almost every
place shows two maximum directions from which winds
blow more frequently than from the other directions, and
that one of these two directions shows a consideiublo excess
over the other. Thus, for example, the following are, on a
twenty years' average, the number of days at Greenwich
each wind prevails during the year: — N., 41; N.R, 49; E.,
23; S.E., 21; S., 34; S.W., 103; W., 38; N.W., 24; and
calms, 32. Hence S.W. and N.E. vrinds are there more
prevalent than winds from any other direction, and of these
two winds the greater maximum direction is S.W. If the
two maximum directions be sorted into groups, then the
greater Tna-nmnm direction occurs as follows : —
from S.S.^V. to W. at 47 places
,, W.K.W. „ N. „ 33 „
„ N.N.E. „ E. „ 19 „
„ E.S.E. „ S. „ 16 „
and the other maximum direction is
from S.S.W. to W. at 20 places
., W.N.W. „ N. „ 22 „
„ N.N.E. „ E. „ 38 „
„ E.S.E. „ S. „ 32 ,,
This result of observation, so different from what was long-
accepted as being in accordance with the generally received
theory of the movements of the atmosphere, teaches the
important lesson that the region towards which the extra-
tropical winds of the northern hemisphere are directed is
not the region of the north pole.
Prevailiiu) Winds in January. — On examimng fig. 14,
which shows the distribution of atmospheric pressure in
January, it is seen that pressure is abnormally low over
the northern portion of the Atlantic — the lowest occurring
between Iceland and South Greenland — from which it
rises as we proceed in a S.W. direction towards America,
in a S. direction over the Atlantic, and in a S.E. and E.
direction over Europe and Asia. Now what influence has
this remarkable atmospheric depression on the prevailing
winds over this large and important part of the earth's
surface 1 The arrows in the figure, which indicate the
prevailing winds, and which have been laid down from
observations, answer this question.
At stations on the cast side of North America the
arrows show a decided predominance of north-west winds;
at the more northern places the general direction is more
northerly, whereas farther south it is more westerly. In
the Atlantic between America and Great Britain, in the
south of England, in France and Belgium, the direction is
nearly S.W. In Ireland and Scotland it is W.S.W.;
in Denmark and the north-west of Russia S.S.W. ; from
St Petersburg to Tobolsk S.W. ; on the west of Norway
generaUy S.S.R; and in Greenland, the north of Iceland,
and about Spitzbergen N.E. Hence all the prevailing
winds in January over this extensive portion of the globe
may be regarded as the simple expression of the difference
of atmospheric pressure which prevails over the different
parts of the region. In truth the whole appears to flow
vorticosely, or in an in-moving spiral course, towards the
region of low pressure Ij-ing to the south-west of Iceland,
and extending ea^twai-d over the Arctic Sea north of Russia.
The only marked changes in these directions of the wind
thus broadly sketched out are the deflexions caused
by the various mountain systems which lie, so to speak,
embedded in these vast aerial ciu-rents ; of these the
winds in the south of Norway afford excellent iUustni-
tions.
The influence which this peculiar distribution of the
pressure over the north of the Atlantic exercises in
absolutely determining the winter climates of the respective
countries is most instructive. It is to this low pressure,
which draws over the British Islands W.S.W. winds
from the warm waters of the Atlantic, that the open, mild,
and, it must be added, rainy winters of these islands are
duo. The same region of low pressure gives Russia and
Western SilK'ria their severe winters ; and it is the same
consideration that fully explains the enormous deflexion of
the isothermal linos from Norway eastwards and south-
PaiWAILING VTOJDS.]
METEOROLOGY
145
eastwards over the Old Continent. Finally, the same low
pressure draws over British America and the United States,
by the N.W. winds which it induces, the intensely dry
cold air-current of the Arctic regions. At Portland, Maine,
which is swept by these cold north-westerly winds, the
normal temperature in January is 23°'6, whereas at
Oorunna, on the coast of Spain, in nearly the same latitude,
where south-westerly winds from the Atlantic prevail, the
mean temperature of the month is 49°-l, or 25°'5 higher.
The region of low atmospheric pressure in the north of
the Pacific is accompanied by prevailing winds over the
region embraced by it and by climatic eflects in all respects
similar to the above. In Vancouver Island the prevailing
winds in January are S.W., at Sitka E.S.E., on Great
Bear Lake E.N.E., in Alaska N.E., in Kamchatka N.N.E.,
and in Japan N.W. In accordance vnth these winds
the winter climate of Vancouver and adjoining regions
is mild and humid, and that of the north-east of Asia dry
and intensely cold.
On the other hand, abnormally high pressure rules over
the continent of Asia at this season, and as regards this
region of high pressure the arrows represent the winds as
blowing outwards from it in all directions. Over the
interior of Asia, where the highest normal pressures are,
observations show a marked prevalence of calms and light
winds, but around this central region the prevailing winds
in January are — at Calcutta N., at Hong-Kong E.N.E.,
at Peking N.W., on the Amur W.N.W., S.E. at Nijni-
kolynisk and S.S.W. at Ustjansk (in t'le north of Siberia),
and at Bogoslovsk S.W. Hence from this extensive
region, where pressure is abnormally high, or where at
this season there is a large surplus of air, the prevailing
winds flow outwards in all directions towards the Ipwer
pressure which surrounds it. Owing to the excessive dry-
ness of the air of Central Asia, terrestrial radiation is less
obstructed there than anywhere else on the globe, and
consequently the temperature falls very low, the mean of
January at Werchojausk being - 55°'8, which is the lowest
mean monthly temperatiwe known to otcur on the earth's
surface. And, since the winds blow outwards from the
dry cold climates of the interior, temperatures are low,
«ven on the coasts. Of this China affords good' illustrations.
Thus the mean January temperature of Peking is 22°'7 and
of Zi-ka-Wei, near Shanghai, 35°'4, whereas at Corfu and
Alexandria the normal temperatures for January are
respectively 50°-9 and SS'-O, or 28°-2 and 22°-6 higher
than i"n corresponding latitudes on the coast of China.
The vdnds of the United States in winter, taken in
connexion with the peculiar distribution of pressure already
described, are very interesting. There are two regions of
high pressure, one in the south-eastern States and the other
and lai-ger one in the region around Utah ; and between
these there is interposed a trough of lower pressure extend-
ing from Chicago to the south-west of Texas. On the
western side of this depression the winds are north-
westerly, but to the east of it they become W., W.S.W.,
and in some places S.W., and again on nearing the Atlantic
seaboard they become north-westerly. In connexion with
the region of higher pressure ir. the west, the prevailing
winds, are seen to flow outward from it. The normal
pressure diminishes everywhere to southward of a lino
drawn from the Canaries to Bermuda, thence westward in
nearly the same latitude to Texas, and then to west-north-
west to San Francisco. The tract of lowest pressiu-e
stretches from the basin of the Amazon in the direction of
the isthmus of Panama in about latitude 8° N., and thence
is continued westward for a considerable distance into the
Pacific in nearly the same latitude. It follows from this
distribution of the pressure that the north trades in a more
,or less modified form prevail over South America to the
16— S
north of the Amazon, and in the Pacific to the north cf
lat. 8° N., probably as far to westward as long. 150° W.
The low-pressiu-e system.^ which prevail during the
summer months in South America and South Africa have
each its corresponding system of -.rinds all roimd. It is,
however, in Australia, as being the most compact and
isolated continent, that the influence of the simimcr sun in
lowering the pressure is best illustrated. Li that continent
the lowest pressure occius in the region situated about
midway between the north coast and the tropic of
Capricorn, over which the normal pressure does not e^iceed
29 '80 inches. Further, everywliere in Australia pressure
diminishes from the coast ou advancing upon the inland
districts. It follows from this disposition of the pressure
that all round the island the prevailing winds in summer
blow from the sea towards the interior ; and accordingly it
is in these months that the greater part of the rain falls.
From the low pressure of the interior southwards to Bass's
Straits pressure rises continuously, the increase in the
normal over this space being o.bout 0'200 inch. To north-
ward it also rises continuously to beyond the north of
China, the increase on this side being about -J of an inch.
In this case the greater part of the increase occurs over
the continent, the rate of increase from the north of
Australia to the Philippine Islands being only about the
rate of increase which obtains southward towards Bass's
Straits. It will be shown when the subject of the rainfall
is examined that it is the relative excess of these higli
pressures, the one in the south of Australia and the other
in the south-east of Asia^ that determines the position
of the area of low pressure in Australia in particular years,
and with that position the degree and extent to which the
whole of the northern portion of Australia is watered by
the rainfall. Thus, when pressure is more than usually
high 'in the south-east of Asia, and either low or not ex-
cessive in the south of Australia, then the low-pressure
region is pushed farther southward into the interior, and
with it the rainfall spreads inland over a wider area and to
a greater depth.
Prevailing Winds in July. — In the winter of the
southern hemisphere, the geographical distribution of
pressure is exactly the reverse in Australia of what obtains
during the summer months. Everyn'here all round it
increases on advancing from the coast into inland districts.
The lowest pressure, about SO'OO inches, occurs on the
north coast, and the highest over the basin of the Murray
river and its affluents, where it rises generally to 30-18
inches. On the south coast it is generally about 30'12
inches, faUing, however, at Gabo Island, in the extreme
south-east, to 30'050 inches, and to 29'836 in the south of
New Zealand. From the Murray river the diminution of
pressure is continuous to the north, even to the low pressure
of Central Asia. From this arrangement of the pressure,
the prevailing winds blow from the interior towards the
surrounding ocean all round Australia, with the single
exception of the extreme south-west of the continent, where
the prevailing winds are south-westerly, being here essenti-
ally an outflow of the high pressiure which overspreads the
Indian Ocean to the westward. As these S.W. winds are
from the ocean, the rainfall at Perth in July is fully 6
inches, and it is high over south-western districts of West
Australia. The prevailing winds round Australia are S.K
on the north coast,' S.W. at Brisbane, W.N.W. at Sydney,
N. at Melbourne, N.E. at Adelaide. These all represent
an outflow from the high-pressure regions of the interior
modified by the influence of the earth's rotation, and, in
correspondence with the reversal of the distribution of the
pressure, are directions the reverse of the prevailing winds
of January.
In July the central and southern parts of Asia ar'.-.
146'
M. E. T E 0 B 0 L O G y
[rKSVAiLiso 'wnrDte
lighly heated b^" the summer sun, and, besides, the rainfall
over southern parts is excessive. Consequently atmospheric
pressure is very low, being fully 0"40 inch lower in the
Punjab tlian it is in the soiitli of Ceylon. From the
interior pressure rises continuously on advancing to the
eastward, southward, westward, and northward, and from
all these directions the prevailing winds of summer flow
inwards upon the interior, and these bring rain or parching
drought according to the vapom- they bring from the
ocean they have traversed, and according as they advance
into warmer or colder regions. The prevailing summer
winds of Asia, being an inflow inwards upon the interior,
have, generally speaking, exactly the reverse direction of
t^t prevailing in winter.
The winds of Europe are mainly determined by the
extraordinarily high pres.siu-e of the Atlantic in its relations
to the low-pressure sy.stems of Central Asia and Central
Africa at this time. The mnds in the Spanish Peninsula
are north-west ; in the north of Africa they are northerly,
and again north-westerly in Syria. The winds of the
British Islands and western Europe have, less southing and
more northing than the prevailing winds of winter, and to
the east of long. 40° E. they become decidedly north-west.
It is to the Atlantic origin of these winds that the summer
climates of these large and important regions owe the com-
paratively large rainfall of this season, it being at this time
that the rainfall reaches the annual maximum. The bear-
ing of the lo^v-pr686ure areas and mountain systems of the
north of Italy and Scandinavia on the climates of these
countries mil be afterwards referred to.
The centre of lowest pressure in North America is over
iKa district about Utah, from which it rises aU round, least
to northward and most in south-easterly and north-westerly
directions. In California N.W. winds necessarily blow in-
-.rardsupon this central low-pressure area; and, as- these winds
pass successively over regions the temperature of which con-
stantly increases, the summer dim;; fo is rainless. On the
other hand, southerly aad south-easterly -winds from the Gulf
of Mexico blow up the western side of the basin of the Missis-
sippi inwards upon the low-pressure area of the centre, de-
positing in their course, in a rainfall more or leos abundant,
the moisture they have brought from the Gulf. To the north
of lat 50°, and to- westward of Hudson's Bay, the prevail-
ing wind.3 become easterly and north-easterly, distributing
over Manitoba, Saskatchewan^ and neighbouring regions,
as they continue their westerly course tov.-ards the low-
pressure area, the rainfall they have transported thither
from the wide expanse of Hudson's Bay. An attentiro
'examination of the arrows of fig. 17 shovvs that the prevail-
ing winds over all the States to the east of the Mississippi
river are rather to be regarded as an outflow from the
region of very high pressure over the Atlantic to south-
eastward. Thus in Florida the winds are S.E., in the
southern States S., and in the lake region, in the New Eng-
land States, and on the Atlantic .seaboard S.W. Since the
origin of these winds is thus essentially oceanic, and since
in their course northwards no mountain range crosses their
path, the whole of this extensive region enjoys a large but
by no means excessive rainfall, which, taken in connexion
with the temperature, renders the smnmcr climate of these
States one of the best to be met with anywhere on
the globe for the successful prosecution of agricultural
industries.
The remarkable protrusion of high pressures from the
southern hemisphere, where they are massed at this time
of the year, northwards into the Atlantic is, as has already
been referred to, one of the outstanding features of the
meteorology of the summer months of the northern hemi-
sphere. In the central area of this large rcgipu the climate
ifi remarkable for its prevailing calms, light winds, occasional
squalls, and clear skies. From this comparatively calm
space the wind blows outwards in all directions towarda and
in upon the surrounding regions of low pressure. These
winds, owing to the high temperature, clear skies, and stro:..:.
sunshine of the region from which they issue, carry with
them a great amount of vapour near the surface, by which
to a large extent the north of South America, the cast of
North America, the greater part of Europe, and a large por-
tion of Africa are watered. The prevailing winds over this
region are further interesting, not merely from the striking
illustration they give of the intimate relation of thfi winii.s
to the distribution of the pressure, but as being of no small
importance in determining the best routes to be taken over
this great highway of commerce, and the more so inasmuch
as the currents of the ocean are coincident with these pre-
vailing winds.
In the Antarctic regions, or rather to the south of lat.>
45° S., the normal atmospheric pressure is low at all
seasons, there being a gradual diininutiou of pressure to
29 '20 inches about lat. 60° S. Pressure is probably even
still lower nearer to the south pole, as seems to be indi-
cated by the observations made by Sir James C Eo.ss, and
in the " Challenger " and other expeditions. Over this
zone the prevailing winds are W.N.W. and N.W. This is
the region of the " brave west winds," the " roaring forties "
of sailors, which play such an important part in navigation,
and which determine that the outward voyage to Australia
be round the Cape of Good Hope and thence eastward, and
the homeward voyage eastward round Cape Horn, the'
globe being thus circumnavigated by the double voyage.:
That the general drift of these ^^'inds is inwards upon the
south pole is strongly attested by the existence of the
enormously thick wall of ice which engirdles these regions,
from which are constantly breaking away the innumerable
icebergs that cover the Southern Ocean, none of which ia
ever seen of a calculated thickness less than 140P feet.;
The snow and rainfall which must take place in the south'
polar regions for the formation of icebergs of such a
thickness must be peculiarly heavy, but not heavier than
might be expected from the strength and degree of satura-
tion of the " roaring forties " which unceasingly precipitate
their moisture over these regions.
To sum up : — so far as the prevailing winds are con-
cerned, it has been sho-nm that wh'.re pressure is high, that
is to say, where there exists a surplus of air, out of such
a region winds blow in all directions ; and, on the other
hand, where pressure is low, or where there is a deficiency
cf air, towards such a region winds blow from all directions
in an in-moving spiral course. This outflow of air-currents
from a region of high pressure upon a region of lov/ pres-
sure is reducible to a single principle, viz., the principle of
gravitation. Given as observed facts the differences of
pressure, it is easy to state with a close approximation to
accuracy what are the prevailing winds, before calculating
the averages from the wind observations. Indeed so pre-
dominating is the influence of gravitation where differences
of pressure, however produced, exist that it may practically
be regarded as the sole force immediately concerned in.
causing the movements of the atmosphere. If there be.
any other force or forces that set the winds in motioiv
independently of the force called into play by differences of
mass or*)ressure, their influence must be altogethfir insig-,
nificant as compared with gravitatioii.
It has been abundantly proved that the wind do,es'notj
blow directly from the region of high towards that of low
pressure, but that, in the northern hemisphere, the region of
lowest pressuio is to the left of the direction to.wards which
tlio wind blows, and in the southern Jiemispherc to the
right of it. . This direction Tof the prevailing tfind with
reference to the pressure is in strict accordance .with I!uya
PREVAILINQ ■WlNDa.J
METEOROLOGY
U7
Pallot's Law of the Winds, which may be thus expressed : —
the wind neither blows round the centre of lowest pressure
in circles, or as tangents to the concentric isobaric curves
of storms or cyclones, nor does it blow directly towards the
centre ; but it takes a direction intermediate, approaching,
however, more nearly to the direction and course of the
circular curves than of the radii to the centre. The angle
formed by a line drawn to the centre of lowest pressure
from the observer's position and a line drawn in the direc-
tion of the wind is not a right angle, but an angle of from
«0° to 80°.
From its importance in practical meteorology Buys
Ballot's law may be stated in these two convenient forms.
(1) Stand with your back to the wind, and the centre of
the depression or the place where the barometer is lowest
will be to your left in the northern hemisphere, and to
your right in the southern hemisphere. This is the rule
for sailors by which they are guided to steer with refer-
iice to storms. (2) Stand with the high barometer to
\ our right and the low barometer to your left, and the
rt-ind will blow on your back, these positions in the southern
hemisphere being reversed. It is in this form that the
prevailing winds of any part of the globe may be worked
out from the isobaric charts (figs. 14 and 17).
From the all-important consequences which flow from the
geographical distribution of the pressure it is evident that
the regions of low and of high normal pressure must be
regarded as the true poles of the prevailing winds on the
earth's surface, towards which and from which the great
movements of the atmosphere proceed. From the unequal
distribution of land and water, and their different relations
to solar and terrestrial radiation, it follows that the poles
of pressure and of atmospheric movements are, just as
happens with respect to the poles of temperature, very far
from being coincident with the north pole. Thus during
the winter months the regions to which the origin of the
great prevailing winds of the northern hemisphere are to
be referred are Central Asia, the region of the Rocky
Mountains, and the horse latitudes of the Atlantic, and
the regions towards and in upon which they flow are the
low-pressure systems in the north of the Atlantic and
Pacific Oceans, and the tract of low pressure within the
ttopics towards which the trade-winds blow. In the
summer months the reversed conditions of pressure-distri-
bution then observed are- attended with corresponding
changes in the prevailing winds ; and, generally speaking,
if the south polar region be excepted, the poles of highest
and lowest pressure and atmospheric movements are at no
time coincident with the north pole. It is this considera-
tion which affords the true explanation why prevailing
winds at so large a proportion of stations in the northern
hemisphere do hot blow in the directions in which true
.equatorial and polar winds should blow.
The causes which bring about an unequal distribution of
the mass of the earth's atmosphere are mainly these two —
the temperature and the moisture of the atmosphere con-
sidered with respect to the geographical distribution of
land and water. Owing to the very different relations of
land and water to temperature, as already stated, the
summer temperature of continents greatly exceeds that of
ithe ocean in the same latitudes. Hence the abnormally
tigh temperature which prevails in the interior of Asia,
'Africa, America, and Australia during their respective
summers, in consequence of which the air, becoming speci-
fically lighter, ascends in enormous columns thousands of
miles in diameter. On arriving at the higher regions of
the atmosphere it flows over neighbouring regions where
the surface temperature is lower, and thus the atmospheric
(jiessure of the highly heated regions is diminished.
Sadsfie 'wicds^set m aU isaiid .to.t^e^:^ p^c.e of t^
air removed from the continents by tKeffeascefiaiig
currents, and since these necessarily are chiefly winds from|
the ocean they are highly charged with aqueous vapour,'
by the presence of which, and by the condensation of the'
■TOpour into cloud and rain, the pressure over continents at
Jhis season is still further and very largely diminished.!
Air charged with vapour is specifically lighter than when
without the vapour; in other words, the more vapour
any given quantity of atmospheric air has in it the less
is its specific gravity ; and, further, the condensation
of vapour in ascending air is the chief cause of the cooling
effect being so much less than that which would be
experienced by dry air. From these two principles^'
which were established by Daltun, Joule, and Sir William
Thomson, it follows that the pressure of vapour in the air,
and its condensation, exercise a powerful influence in
diminishing the pressure. The great disturbing influences
at work in the atmosphere are the forces called into play,
by its aqueous vapour ; and it is to these, co-operating with
the forces called into play by the differences of temperature
directly, that the low normal pressure of the continents
during the summer is to be ascribed. The degree to which
the lowering of the pressure takes place is, as was to have
been expected, greatest in Asia, the largest continent, and
least in Australia, the smallest continent, while in America
it is intermediate.
The influence of the aqueous vapour in diminishing the
pressure is well seen in the belt of calms in the tropica
between the north and the south trade-vrinds. Since these
winds import into the belt of calms the vapour they have
taken up from the sea on their way thither, the climate ia
characterized by a highly satm-ated atmosphere and heavy
rains. Again the air in regions near the Atlantic contains
much more vapour and is of a higher temperature during
winter than is observed at places in the interior of con-
tinents in the same latitudes. It follows thus that the air
over the north of the Atlantic and the regions adjoining is
specifically lighter than in the regions which surround
them. We have here therefore the physical conditions of
an ascending current ; and it is plain that the strength of
this current will not merely be kept up but increased by
the condensations of the vapour into cloud and rain which
take place within it, by which a higher temperature and a
greater specific lightness are maintained at the surface of
the earth and at various heights in the atmosphere than
exist over surrounding regions at the same heights.
Accordingly it is seen from the winter isobars that an
enormous diminution of pressure occurs over these regions,
and also over the north of the Pacific and the Antarctic,
as compared 'with the continents.
Since, on the other hand, dry. and cold air is specifically,
heavy, the winter isobars show that where temperature ia
low and the air very dry pressure is high. Of this Asia
and North America are striking examples during December,
January, and February, and Australia, South Africa, and
South Ajnerica duri^ig June, July, and August.
Since vast volumes of air are thus poured into the region
where pressure is low without increasing that pressm-e, and
vast volumes flow out of the region where pressure is high
without diminishing that pressure, it necessarUy foUows
that the volumes of air poured into the region of low
normal pressure do not accumulate over that region, but
must somehow e-scape away into other regions, and that
the voltmies of air which flow out from the region of high
normal pressure must have their place supplied by fresh
accessions of air poured in from above. That the same
law of relation observed between sea-level pressures and
surface winds obtains between pressures at different heights
and winds at the same heights is simply a necessary
inference. ^We„»re therefore justiledJ&jJjiectingthftt.
148
METEOKOLOQY
[pEEVAlLrNO 'wasft
ascending currents \'nil continue their ascent till a height
is attained at which the pressure of the air composing the
currents equals or just falls short of the pressure over the
Eurrouuding regions at that high leveL On reaching this
height the air, no longer buoyed up by a greater specific
levity than that of the surrounding air, will cease to
ascend, and expanding horizontally will thenceforth flow
over as an upper current towards those regions which offer
the least resistance to its course ; that is to say, it will
flow over upon those regions where, at that height, pressure
happens at the time to be least. Now from the known
densities of air of different temperatures and humidities it
is evident that the overflow of the upper current will take
place towards and over that region or regions the air of
which in the lower strata of the atmosphere happens to be
colder and drier than that of the otTier surrounding
regions, — because, being denser, a greater mass of air is
condensed or gathered together in the lower strata of the
atmosphere, thus leaving a loss mass of air, or a diminished
pressure, in the higher region of the upper current.
If this be so, then the extraordinarily high pressure of
Central Asia during winter is to be ascribed to these two
causes :— (1) the low temperature and excessive dryness of
.the air of this extensive region ; and (2) its relative
Broximity to the low pressure of the Atlantic to the north-
west, the low pressure of the Pacific to the north-east, and
the low pressure of the belt of calms to the south.
Similarly, since in summer the temperature of air resting
over the Atlantic between Africa and the United States is
much lower than that of the land, the ascending currents
which arise from the heated lands of Africa, Europe, and
North and South America, as well as from the region of
calms immediately to the south, all of which are remark-
able for a low normal pressure, will on reaching the upper
regions of the atmosphere flow towards this part of the
Atlantic, because there, the temperatm'e being lower and
the density of the air composing the lower strata being
greater, pressure in the upper regions is less. And, since
the surface winds are constantly flowing outwards from
this region of abnormally high pressure, thus draining
away the air poured down ujxm it by the upper currents
which converge upon it, extreme saturation does not take
place, and the air consequently is relatively dry and cool.
That this view generally represents the movements of the
upper ciirients has been strongly confirmed wjthiu the last
few years by Professor Hildebrjmdsson and Clement Ley
in their researches into the upper current of the atmosphere
based on observations of the cirrus cloud.
From these considerations it may be concluded that the
winds which prevail near the earth's surface are known
from the isobaric lines, the direction of the wind being
from regions where pressure is high towards regions where
it is low, in accordance with Buys Ballot's law ; and that
the upper currents may be inferred from the isobaric lines
taken reversely, together with the isothermal lines taken
directly. In other words, the regions of lowest pressure,
with their ascending ciirrents and relatively higher pressure
at great heights as compared with surrounding regions,
point out the sources or fountains from which the upper
currents flow ; and the isothermals, by showing where on
account of the relatively low temperatures the greater
mass of the air is condensed in the lower strata of the
atmosphere and sea-level pres.sure consequently is high,
thus diminishing the pressure of the upper regions, point
out the regions towards and upon which these upper
currents of the atmosphere flow. The facts of the diurnal
oscillations of the barometer in the different regions
already discussed afford the strongest corroboration of these
news.
The term " monsoon " has long been applied to tho pro-
vailing winda in southern Asia wliich blow approximately
from S.W. from April to October, and from N.E. from
November to April. The term is now, huv.-ever, generally
applied to those winds connected with continents which
are of seasonal occurrence, or which occur regularly with
the periodical return of the season. Since they are caused
immediately by the different temperatures and prcssurea
which form marked features of the clJjuates of continents
in winter and summer respectively, they are most fully
developed round the coast of Asia, owing to the great
extent of that continent. The monsoons of dijffereat parta
of the coasts of Asia differ w-idely in direction from each
other. Thus in winter and summer respectively they are
W.N.W. and E.N.E. at the mouth of the Amur, H. and
S.S.E. at Shanghai, N.E. and S.W. at Rangoon, N. and
W.S.W. at Bombay, N.W. and S.W. at Jerusalem, and
S.S.W. and N.N.E. at Archangel. The Indian winter
monsoon generally begins to break up in Starch, but it is
not til! about tho middle of May, when the normal pres-
sure has been decidedly diminished over the heated
interior, that the summer monsoon acquires its full strength
and the heavy raonsoonal rains fairly set in. In October,
when the temperature has fallen considerably and with
the falling temperature the pressure of the interior has risen,
the summer monsoon begins to break up, and this season
is marked by variable winds, calm.s, and destructive
hurricanes. As the temperature continues to fall and
pressure to rise, the winter monsoon again resumes its
sway. Monsoons, equally with the trade-winds, play a
most important part in the economy of the globe. The
relatively great force and steadiness in the direction in
which t'ney blow, and the periodical change in their direc-
tion, give facility of intercourse between different countries ;
and, besides, by the rainfall they bring they spread fertility
over exteiisive regions which otherwise would be barren
wastes.
The winds of Australia are also strictly monsoonal, but
owing to the small extent of that continent, and coiise-
quently the smaller differences there are between the
normal pressure of the interior and that of the surrounding
coasts in summer and winter respectively, they are less
strongly marked than are the monsoons of southern Asia ;
and particularly they neither blow with the same force nor
so steadily from the same point of the compass. For the
same reason the Australian climates are characterized by
the' occurrence of more frequent droughts than are the
climates of southern Asia, and the same remark applies to
tno climates of southern Africa.
Since the Malay archipelago lies during ti?3 summer of
the northern hemisphere between tho high pressure o£
central Australia and the low pressure of Asia^ and during
the winter between the high pressure of Asia and the low
pressure of central Australia, it follows that the winds of
the.se Islands are emihently monsoonal in their character,
being in summer southerly and in winter northerly. The
result of this peculiar wind system of the archipelago is to
give to these islands a singular diversity of climates, which
will be more particularly referred to under rainfall.
At Zanzibar the prevailing wind in July is S.E., but in
Jauuary, when tho low pressure of the interior is situated
much farther to southward, it is N.E. : and tho same
influence is felt, though in a greatly modifled degree, as
far as Mauritius, where the S.E. trade changes nearly into
R during the summer. On the other side of Africa the
S.E. trade of the South Atlantic is changed into a S.W.
monsoon on the coast of the Qulf of Guinea.
In the southern, central, western, and northern regions
of North America the prevailing winds have a well-marked
monsoonal character. The prevailing winds of winter and
summer respectively are N.E. and S.S.E. at New Orleans,
TPBEVAILINO WINDS.]
METEOROLOGY
149
N.W. and S.W. in Utah, N. and S. at Fort Yuma
(California), E.S.E. and N.W. at Portland (Oregon), and
S. an4 E.N.E. at Fort York, Hudson Bay. These winds
are readily accounted for by the distribution of pressure
«ver the continent in winter and summer. On the Atlantic
seaboard of the United States the prevailing winds of
winter vary from N.W. in the New England States to W.
in South Carolina ; whereas in summer they vary generally
from S.S.W. in South Carolina to S.W. in the New Eng-
land States. Hence over the eastern States the summer
winds are not directed towards the low-pressure region of
the interior of the continent, but are determined by the
relations of their pressure to the high pressure of the
Atlantic to the eastward, and to the lower pressure over-
spreading the Atlantic to the N.E. This influence of the
/.tlantic may be considered as felt westward through the
States as far as the Missiesippi.
Though not so decidedly marked, tne winds of Jturope,
except the extreme south, are ako monsoonal. In winter
they flow from the land towards the region of low pressure
in the north of the Atlantic ; but in summer the arrows,
representing the prevailing mnds, show that all but the ex-
treme south of Europe is swept by westerly winds, which flow
in a vast continuous stream from the Atlantic towards the
central regions of the Old Continent, and which deposit in
their course the rains they have brought from the ocean.
Similarly, monsoons prevail on the coasts of Brazil,
Peru, North Africa, and many other regions which happen
1o lie between other regions whose temperatures, and
therefore pressures, differ markedly from each other at
di£ferent times of the year.
These are the chief prevailing winds of the globe when
the differences of the normal atmospheric pressure are such
as to cause a decided and steady movement of the atmo-
sphere over a large portion of the earth's surface, resulting
in well-marked prevailing winds. But there are other
winds which are greatly influenced by local causes, such as
the nature of the ground, whether covered with vegetation
or bare ; the physical configuration of the surface, whether
level or mountainous ; and the vicinity of extensive sheets
of fresh or salt water. An important characteristic of
winds in their practical relations to climate is their
quality, — they being warm or cold, dry or moist, according
to their direction and the nature of the earth's surface
over which they have just passed. Thus in the northern
hemisphere southerly winds are warm and moist, while
northerly winds are cold and dry. In Europe south-
westerly winds are moist and easterly winds dry, while in
the New England States and Canada north-easterly winds
are cold and raw and north-westerly winds cold and dry.
In particular regions certain meteorological conditions
occur at stated seasons intensifying these effects, resulting
in e.tcessive drought, heavy raius, intense or great heat,
thus giving rise to the following among other well-known
winds. The east winds of the British Islands occur chiefly
in spring, but also in a less degree in November, being in
the latter case often accompanied with fog. The winds
here referred to are dry and parching, and their deleterious
influence on the health is seen, not merely in the discomfort
and uneasiness they impart to the less robust of the popu-
lation, but also in the largely increased mortality which
they cause from consumption and all other diseases more
or less connected with the nervous system. In the
countries bordering on the north of the Atlantic, atmo-
spheric pre.ssure reaches the annual maximum in May, and
it is above the average during the other two spring months.
In these months the normal pressure approaches nearer to
what obtains farther south, and an examination of daily
weather maps shows that this is due to the repeated
«oeurrence in spring of very high pressures in the north of
Europe wnile pressures much lower prevail to southward.
Now these east winds are simply the outflow from these
regions of high pressure to northward. Northerly and even
westerly winds which are truly outflows from what may be
styled Arctic anticyclonic areas bring -n-ith them qualities as
noxious as those of the east wind itself, and prove as injuri-
ous to health and vegetation. The cold dry wind of April
29, 1868, which blasted and shrivelled up vegetation in Scot-
land, particularly in the western counties, as effectually as
if a scorching fire had passed across them, was a west wind.
In tho south of Europe, during the winter and early spring,
peculiarly diy, cold, and violent northerly winds are of occasional
occurrence. Of these winds the "mistral" is one of tho most
notorious, which is a steady, violent, and cold north-west wind
blowing from central and eastern France down on the Gulf of
Lyons. It is particularly trying while it lasts to invalids who are
spending the winter at the various popular sanatai-ia which are
scattered along this part of the Mediterranean coast. The great
cold that took place in the north of Italy and south of France in
the beginning of 1S68 was a good example of the mistral. Tho
meteorological conditions under which it occurred were unusually
low pressure over the Mediterranean to southward (29-450 inches),
whilst at the same time pressure rose steadily and rapidly on pro-
ceeding northward to 30 905 inches in the north of Russia. From
this geographical distribution of the pressure, northerly winds st. apt
southwards over Europe, carrying with them the low temperatures
of tho higher latitudes, and became still colder and drier on crossing
the Alps before they made the descent on the shores of the Mediter-'
ranean. The cold tempestuous winds which descend from the JuliaD'
Alps and sweep over the Adi-iatic, and the dreaded "gregalo" of
Malta, which is a dry cold north-east wind, are in their character
and origin quite analogous to the mistral.
The " northers," or "nort«s," are peculiarly dry cold strong windi
which repeatedly occur from September to March in tho Statea
bordering on the Gulf of Mexico, and are perfectly analogous to the
mistral. The condirions under which tuey occur are a pressure
lower than usual to the south or south-east over the Gulf of Mexico,
together with a pressure even higher than the high normal which
is so marked a feature of the meteorology of the Rocky Mountains
during the colder months. When, as most frequently happens,
they occur in the wake of a storm, their disagreeable qualities of
extreme dryness, cold, and violence are all intensified. From a
temperature of upwards of 80° experienced as the storm comes up
the thermometer rapidly falls to 18° or even lower ; and, as the low
temperature often occurs mth a wind blomng with great violenee7
the northers prove most deleterious. A violent wind with a tcn»-
oerature of 18° is altogether unknown in the British Islands.
Tho " pampero " is a stron:;, dry, cold wind which blows across the
pampas of the River Plate of South America, occurring at all seasons,
but most frequently duriu" the spring and summer from October to
January. They are preceded by easterly winds, a falling pressure,
a rising ternperature, and increased moisture. A pampero is de-
scribed by Dr D. Christison, and its appearance figured, in the
Journal of the Scottish Mclcorolo'jkal Soculy, vol. v. p. 342, as seen
advancing on the morning of November 28, 1867, in central
Uruguay. In the early morning the wind blew rather strongly
from north-east, and by and by clouds were seen moving very
slowly from tho west, throwing out long streamers eastwards. A«
they advanced, two dense and perfectly regular cloud-masst-s
appeared in front, one behind the other, in close contact yet not
intermingling, — the one being of a uniform leaden grey, while thd
other was as black as the smoke of a steamer. On arriving over-
head, the front, though slightly wavy in appearance, was seen to be
quite straight in its general direction, and the bands were of uniform
breadth. They rushed forward at grcit speed under the other
clouds without uniting with them, preser\'ing their foims unbroken,
being borne onward by an apparently irrcsibtible force, as if com-
posed of some solid material rather than vapoun They extended
probably 50 miles in length, but as they took only a few minutes
to pass their breadth was not great, and they appeared to diminish
to mere lines in the distant horizon. At the instant the first cloud-
band arrived overhead, the wind chopped round from north-east to
north and then to south-west; a strong cold blast at the same time
seemed to fall from the leaden cloud, and continued to blow till
both bands had passed. No rain or thunder occurred at this time,:
but in the confused rabble of clouds which followed low thunder
continued to roll, and in a quarter of an hour rain fell, and for some
hours thereafter wind, rain, and thunder continued, but only to s
moderate degree. The low temperature and rising barometer and
change of wind are the constant and most striking characterisricg
of the pampero. On one occasion the temperature fell 44* in four-
teen hours, and on another occasion the fall was only 4°. Rain ia
a usual accompaniment, but on rare otcaaions the pamj^ro passes o9
and no tain falls.
150
METEOROLOGY
LaiiiiFALij
Rainfall. — Wliatever tends to lower the temperature of
the air below the dew-point is a cause of rain. It is there-
fore to the winds we must chiefly look for an explanation
of the rainfall, and the broad principles of the connexion
may be stated to be these five : — (1) when the winds have
previously traversed a considerable extent of ocean, the
rainfall is moderately large ; (2) if the winds advance at
the same time into colder regions, the rainfall is largely
increased, because the temperature is sooner reduced below
the point of saturation ; (3) if the winds, though arriving
from the ocean, have not traversed a ownsiderable extent of
it, the rainfall is not large; (4) if the winds, even though
having traversed a large extent of ocean, yet on arriving
at the land proceed into lower latitudes or regions markedly
warmer, the rainfall is small or nil ; ;(6) if a range of
mountains lies across the onward path of the winds, the
rainfall is largely increased on the side facing the winds,
and reduced over the regions on the other side of the
range. The reason here is. that, the air on the windward
side of the ridge being suddenly raised to a greater
height in crossing the range, the temperature is further
reduced by mere expansion, and a more copious precipita-
tion is the result ; whereas on the leeward side as the air
descends to lower levels it becomes gradually drier, and
accordingly the rainfall rapidly diminishes with the
descent.
We have drawn attention to the dimiuished velocity of the wind
over land as compared with the open sea (p. 125). From this it
follows that an envelope of stiller air or air of less velocity than
that of the . prevailing wind broods over the land, and by its
presence forces the prevailing wind to a greater height, thus tending
to increase the rainfall. It the foreshore rises within a few milos
to a height of 200 or 300 feet, the result is very striking when tlie
wind from the sea blows straight upon it. Thus at Spittal; near
Berwick, on September 1877, a N.E. wind blew .straight ashore at
an estimated velocity of 25 miles an hour. To eastward the sky
was singularly clear down to the horizon, but to westward all the
country beyond a mile from the shore was enveloped in what
appeared a dense mist or fog. About 16° to eastward of the zenith
of an observer on the shore, the thinnest rack of cloudlets was seen
emerging without intermission from tlio deep stainless blue of the
sky, which as they drifted landward increased so rapidly iu vulume
and density that the zenith was three-fourths covered with clouds.
A similar phenomenon was seen in September 1879 on board the
Orkney steamer at the magnificent cliff of Hoy Island, Orkney.
A heavy storm had just cleared away, and a strong W.N.W. wind
was blowing right against the cUif. The sky was absolutely cloud-
less all round, except the upper 300 feet of Hoy Hill, 1570 feet high,
which was enveloped in a tliick mist that stretched away to wind-
ward, some distance to westward of the steamer's course, which
was about 2 miles from land. The western termination of the
cloud was the thinnest rack of cloud, which emerged unceasingly
from the blue sky at a distance not less than i miles to wind-
ward of the clilf. The constituent parts of the cloud itself were in
rapid motion eastward, but, owing to the fresh accessions it was
constantly receiving, the cloud itself appeared stationary. Thus
the wind was forced upward into tlie atmospliero for some consider-
able distance to windivard of the ridge lying across its path.
It is this dragging effect of the land on tlie wind, and the con-
sequences which result from it, that explain how it is that during
storms of wind and rain from the north-east tiie rainfall over the
foreshores of the Firth of Forth, the Moray Firth, and the Pentland
Firth looking to the north-east is so much in excess as compared
with the rest of Scotland. Tlie same principle explains the heavy
rainfall in plains at some distance from the range of hills lying
across the wind's path and on tlie side of the rain-bringing winds.
For short intervals of time the heaviest rainfalls occur
with tornadoes, waterspouts, and some other forms of the
whirlwind, the reason being that not only is there rapid
expansion due to the rapid ascent of the air, but also great
rarefaction is produced by the extreme velocity of the
aerial gyrations round the axis of the tornado. On August
1, 1846, 3-12 inches of rain fell at CamberweJl, London,
in two hours and seventeen minutes. Of heavy falls
may be mentioned 4'60 inches in London, April 13,
1878; 600 inches at Tongue, September 7, 1870; 0-36,
Anchos in Monmouthshire, July 14, 1875; 6-62 inches at
Seathwaite, Cumberland, November 27, 1848; and 712
inches at Drishaig, Argyllshire, December 7 to 8, 1863.
But it is in lower latitudes that the heaviest single showers
have been recorded. The following are among the most
remarkable : —at Joyeusc, France, 31 -17 inches in twenty-
two hours; at Genoa, 30-00 inches in twenty-four hour.,; at
Gibraltar, 33'00 inches in twenty-six hour.s; on the hills above
Bombay, 24-00 inches in one night ; and on the Khasi
Hills, India, 30-00 inches on each of five successive days.
As regards the ocean, there are no available data from
which an estimate could be formed as to the amount
of. the rainfall, since the rainfall statistics of the ocean
must be regarded as giving hardly anything more than
the comparative frequency of the fall. It is, however,
certain that the equatorial belt of calms in the Atlantic
and Pacific between the trades is the region where the ocean
rainfall reaches the maximum, and the parts of these
oceans are the rainiest which are the longest within the
belt of calms as it shifts its position northward and south-
ward ^vith season. While the cloud-screen is undoubtedly
dense, and the rainfall frequent and heavy, the careful
observations of the "Challenger" and "Novara" show
that the statements generally made as to these ooints are
greatly exaggerated.
In the regions of the trades the rainfall is everywhere
small over the open sea, seeing that the trade--winds are
essentially an outflow from anticyclonic regions, and their
original dryness is to a largo extent maintained becau.-^o
their course is directed into regions which become con-
stantly -narmer. Thus at Ascension, lat. 8° 45' S., which
is throughout the Avhole year within the S.E. trades, the
mean rainfall for the two years 1854-55 was only 8-85
inches. At St Helena, which lies constantly within the
same trades, five years ,give a meai/ rainfall of 5-3G inches
on the coast; but in the same island at a height of 1763
feet the annual amount rises to 23-98 inches. Maiden
Island and some other islands in the Pacific, about loifg.
150° W., and for some distance on each side of the equator,
have been pointed to by Scott as practically almost rain-
less, as is shown by their containing extensive guano
deposits. These islands are situated somewhat similarly
to Ascension with respect to the zone of calms. In
Mauritius the annual rainfall on a mean of four years
was 30 inches at Oros Cailloux, but at Cluny, only 16
miles distant, for the same four years it was 146 inches:
in regard to which Meldrura remarks that at Cluny, -which
is in the vicinity of mountains and forests, in the south-
east of the island, . and thus directly exposed to the trade-
■svind as it arrives from the sea, the rainfaU in almost any
month is from four to six times greater than at Gros
Cailloux on the north-west coast, where neither mountain
nor forest exists, and where the S.E. trade arrives con-
siderably drained of its moisture.
From what has been said it is e-vident that the heaviest
rains will bo brought by the winds which have traversed
the greatest extent of ocean within the tropics, and which
accordingly of all ocean winds have the highest temperature
and humidity. These conditions are most completely
fulfilled during the summer months of the northern
hemisphere by the \^inds -nhich, commencing from near
lat. 30° S., blow home on southern Asia a^ the well-kno-wn
S.W. monsoon of these regions. Accordingly it is by the
winds of this monsoon that a larger rainfall is distributed
over a larger portion of the earth's surface than occurs
anywhere else in any season; and this large rainfall is
in many regions still farther greatly increased by the
mountain ranges -which lie across the path of the rain;
bringing winds.
It is on these -winds th&t the rainfall of India chiefly
depends. Along the wholo of the woet coast from the
KADTFALL.]
METEOROLOGY
151
Qulf of Cambay southward, and on the Western Ghats,
the rainfall is excessive. The following are some of the
more interesting annual means in inches beginning with
Bombay and proceeding southwards : — Bombay, 74 ;
Matheram, 247 ; Mahabaleshwar, 252 ; Ratnagiri, 104 ;
Baura, 255; Goa, 102; Karwar, 115; Honawar, 139;
Mangalore, 134; Cannanore, 132; Calicut, 116; and
Cochin, 114. Ip the west of Ceylon the rainfall is also
heavy, being at Colombo 87, at Galle 91, and at
Ratnapura, at some distance inland among the hills, 149.
Since the S.W. monsoon is drained of much of its
moisture in crossing these mountains, a greatly diminished
rainfall is distributed over the interior and east side of
India, and on the eastern slopes of Ceylon.
If now we cross to the eastern shores of the Bay of
Bengal, we again encounter an excessive rainfall along these
coasts and up the slopes of the mountains looking down on
them. Thus from south northward the following are
among the more characteristic rainfaUs in inches : —
Nancawry, 102; Port Blair, 116; Mergui, 152; Tavoy,
196; Maulmain, 189; Rangoon, 100; Bassein, 98;
Sandoway, 212; Akyab, 198; and Chittagong 104. On
the other hand, at Thyetmio, inland on the Irawadi, the
annual rainfall i.=i only 48 inches.
We have shown how, in accordance with the peculiar
distribution of pressure in India in svunmer, the monsoon
is diverted up the valley of the Ganges as an E.S.E. wind,
distributing on its way, even to the head of the valley, in
a generous rainfall the moisture it has brought from the
Indian Ocean and the Bay of Bengal. The rainfall does
not extend far'the westward than the basin of the Ganges,
and the precipitation ia most copious along the lower
Himalayas, the largest falls being recorded at heights
about 4000 feet, — being, as pointed out by Hill, near the
level at which the summer monsoon is cooled just below
its dew-point. The following are some of the larger rain-
falls in inches, beginning with the more western: — Mus-
sooree, 95 ; Naini Tal, 92 ; Khatmandu, 57 ; Darjiling,
121 ; Kurseong, 154; Buxa, 219; Kuch Behar, 131.
The rainfall is very large in the north-east angle of the
Bay of Bengal and thence northwards towards Bhutan, or
at the angle where the summer monsoon from the bay
curves round to a westerly course on its way up the
Ganges. Thus at Koakhally, on the coast, it amounts in
inches to 109 ; at Tura, on the Brahmaputra, immediately
to west of the Garo Hills, 129; at Silchar and Sylhet to
eastward, 117 and 155; whilst at Cherrapunji, on the
Khasi Hills, it rises to 493-l'9 inches on a mean of twenty-
four years. This last rainfall is the largest known on the
globe, the causes of which are the highly saturated state
of the monsoon on its arrival at the lower Ganges, the
high mountain range of Burmah to eastward of Bengal,
which turns the monsoon to the north, and the protrusion
westwards of the Khasi and Garo HUls so as to lie in the
line of that branch of the monsoon which passes from the
lower Ganges into the basin of the Brahmaputra above
Goalpara. The consequence is that the highly saturated
ail' of the monsoon in its passage across the Ivhasi Hills is
suddenly raised to a height of about 6000 feet, and being
thereby reduced far below the point of saturation the
superabundant moisture is precipitated in unequalled
deluges of rain. The amount of the annual rainfall at all
these places is determined, essentially if not altogether, by
the rains of the summer monsoon, the relative intensity of
Tvhich over India may be taken to be fairly represented by
'the rainfall of July.
The rains which accompany the N.E. monsoon of the
winter months may bo represented by the rainfall for
JaKiary. These are heaviast in Ceylon, especially on its
gast slopes, and in southern India, or where the N.E.
monsoon arrives sfttir having tra.arsod a large extent of
ocean. The fall for the month exceeds 6 inches over ji
large portion of the east coast, whilst at Colombo in the
west the rainfall is only half that amount, and farther north
at Pattalum the Januar}- rainfall is only 1'82 inches. lu
southern India the amount varies from about 1 to 2 inches.
Blanford pointed out in 1873 (Phil. Tram., vol. cLxiv. p.
618) that, while the surface windsof northern India in win-
ter are northerly, on the Himalayas, especially the nortli-
west portion, southerly winds prevail during the cold month.s.
It is these upper southerly winds which bring the winter
rains to the Punjab, Upper Itdia, and the highlands of
Assam. It is further to be noted that wnter rains also
occur in Central India, where the prevailing surface winds
are from east and north-east. The mean rainfall of January
at Mussooree is 2'00 inches and at Naini Tal 2'86 inches,
and in Assam, at Sibsagar, 1'13 inch. Over a large tract
of the east side of southern India from NeUore southward,
including Ceylon, the maximum rainfall for the year occurs
in the months of October and November.
Rainfall of tlie Malay Archipelago and Australia. — Uudcr the
direction of the late Dr Bergsma, systematic observations of the
rainfall of the Slalay archipelago were begun in 3879, the number
of stations being 150. The results of the first three years show that
the mean annual rainfall over the arcliipelago varies from about 60
inches in Timor to upwards of 200 inches at some spots among the
western slopes of Sumatra. But the most important feature in tljo
rainfall in its relations to climate is not the absolute amount that
falls annually, but rather the manner of its distribution through
the months of the year. Over the greater number of the islands
rain falls copiously every month; but as regards some of the islands
the year is divided into dry and wet seasons as marked as are seen
in the climates of India. The key to this essential dilTerence among
the climates is the distribution of atmospheric pressure during tho
months of the year from south-eastern Asia to Australia; with the
resulting prevailing winds. During the winter months atmospheric
pressure is high in south-eastern Asia and low in the interior of
Australia, the difference being about three-quarters of an inch.
Since between these tvio regions the fall in tho mean pressure is
practically uninterrupted, the Malny archipelago lying between
them is swept by northerly winds (fig. 14). As these winds have
traversed a great breadth of ocean in their course, they arriVe in a
highly saturated state, and consequently deposit a copious rainfall,
particularly on the northern slopes of the higher islands. Hence
in these months the rainfall over the islands without exception is
large, the mean monthly amount being in many cases more than 30
inches. These winds continue their course to southward towards the
low-pressure region in the interior of Australia, and deposit along the
north coasts of that continent a monthly rainfall rising generally
to from 14 to 20 inches. On advancing into the interior, the mean
amount gradually diminishes at the successive telegraphic stations
to 3 "50 inches at Alice Springs near the tropic of Capricorn. The
amount of the rainfall for any particular year, and the distance from
the coast to which the rains penetrate inland, depend essentially on
the height of the winter pressure of south-eastern Asia as compared
with tho low mean pressure of central Australia, by which the
strength of the northerly monsoon is regulated.
On the other hand, during the summer of the northern hemisphere
pressure is high in the interior of Australia and low in China, the'
mean difterence being about half an inch. Between the two regions
the fall in the mean pressure is continuous and uninterrupted, and
as a consequence southerly winds prevail over the intervening archi-
Eelago. These winds, as they advance from the continent into lower
ititudes, are absolutely rainless in the north of Australia, and over
Timor and the other Malay islands which arc separated from
Australia only by a comparatively narrow belt of sea. During the
three years no rain whatever fell in Timor in July and A igust, and
tlie fall in June, September, and October was small. As, however,
the winds pursue their course to northward, they 'agerly lick up
moisture from the sea, so that by the time they arrive at Aniboyna
they have become so saturated that the monthly rainfall there rises
to nearly 30 inches. Again at some distance to the west of Timor
rain falls more or less regularly every month, the amount inci'eas-
ing in proportion to the extent of ocean traversed by tho S.E.I
winds, which advance towards these islands from the direction of
Australia. These marked differences among the climates of tho
Malay archipelago, which, since they really dep-'nd on the geo-
graphical distribution of land and sea of this part of the glote, must
be regarded as permanent differences, have played no inconspicuous
part in the singular distribution of animal and vegetable life which
characterizes the archipelago.
152
METEOROLOGY
[P.AI:!! .iXJ,
In July tlio prcTailins wind in West Australia is N.W., and the
miiifall riachcs the maximinn for tho year, whereas in January tha
wind is H. E., and tho rainfall is the minimum. Similarly in
January since tho winds of the southern half of South Aastralia and
Victoria are from the south, and thus blow towards warmer regions,
tho rainfall is eitlier at the annual minimum, or it is small. But
on rounding the coast and proceeding northward, the wind becomes
E. , then N. E., and ultimately N. in the north of Queensland.
Willi this pri'valence of oceanic and equatorial winds, the rainfall
at this time of the year rapidly rises over the whole of tlio eastern
.slopes, till at Capo York it is about 20 inches. In tho basins of tho
Murray and Darling rivers, which are shut off from tlie cast by tho
mountain ranges of Now South Wales, the rainfall is only about an
inch and a half. On the other hand, to south of the latitude of
Sydney, including Tasmania, the maximum rainfall occurs in winter
over tliose regions which slope south towards the sea. On crossing
the mountain range of Victoria into the basin of the Murray river,
the rainfall rapidly diminishes. In the north of New Zealand the
winter rainfall is the heaviest; but farther south, where westerly
winds prevail with some steadiness through the year, the rainfall is
more equally distributed through the months ; and, as the prevailing
winds are westerly, the heaviest rainfall is in the west of the islands.
Thus at Hokitika in the west near sea-level, and not far from a lofty
range of mountains to the east, the annual amount reaches 120
inches, and at Bealey inland at a height of 2104 feet it is 106
inches. At Wellington the annual rainfall is 52 inches, at
Southland 46, at Dunedin 34, and at Christchuroh 25, thus
showing, in the rainfall of the two sides of the island, extremes
nearly as great as in Scotland.
Rainfall of Europe. — As regards roinfaU, Europe may be
conveniently divided into two distinct regions, — western and
northern Europe, extending in a modified degree througli
the interior of the continent into Siberia, and the countries
bordering on the Mediterranean. A vast ocean on the one
hand, a great continent on the other, and a predominance
of westerly winds are the determining circumstances in the
distribution of the rainfall over western Europe. Hence
the rainiest regions are to be found in the west, where
mountain ranges stretch north and south. The annual
rainfall exceeds 80 inches over a considerable district,
including the greater part of Skye and portions of the
counties of Inverness and Argyll to the south-east, in the
lake district of England, and in the more mountainous
parts of North Wales, — these three districts being the
wettest in Europe. As Ireland presents no continuous
range of mountains opposing the westerly winds of the
Atlantic, no Irish rain-gauge shows a mean rainfall of 80
inches. A point of some interest is suggested by the rain-
fall of the counties of Kirkcudbright and Dmnfries in
Scotland. These counties offer to the westerly winds a
series of valleys sloping south to the Solway Firth, which
show successively a diminished rairtfall on advancing east-
ward till at several places in Nithsdale and Annandale it
does not exceed 40 inches. But in Eskdale, farther to the
tast, the rainfall instead of falling increases to about CO
inches. The reason is that the westerly winds are
obstructed in their onward course by the range of hills by
which Eskdalo is bounded on the east, in surmounting
which tho ^vind3 are much reduced in temperature, and their
superabundant moisture falls iu copious rains immediately
to westward of the ridge. The cause of tho larger rainfall
of Eskdale is thus analogous to that of the large rainfall
i^f tho coast in the north-east of the Bay of Bengal
immediately under the Assam rango of mountains. In
England the largest annual rainfall is 140 inches at Soa-
thwaite in the Lake district, in Scotland 128 inches at
• jlencroe in Argyll, whilst in Ireland the largest is only
70 inches. The driest part of tho British Islands is an
extensive district to south-south-west of the Wash, with a
rainfall of about 21 inches. A large extent of England,
and all the more important agricultural districts in Scotland,
have a rainfall under 30 inches : the greater part of
England, and nearly tho half of Scotland, liavo a rainfall not
exceeding 40 inches ; but in Ireland it is isolated patches
only that show a rainfall less than 40 inches.
In tho west of Norway the rainfall iu inches is 72 at
Bergen, 51 at Aalesund, 40 at the Naze and in the Lofoten
Isles, falling to 10 at tho _,'orth Cape. At Christiania,
Upsala, and a large part of the east of Scandinavia tho
rainfall is about 21 inches, falling to 16 inches on the
north coast of the Gulf of Bothnia. In Russia and Siberia
it rises only at a few places to 20 inches, several di.^tricta
of this extensive region having an annual rainfall of 10, 5,
3, or even 2 inches. The rainfall of Spain presents great
ortremes — from 68 inches at Santiago to 13 inches .at
Saragossa. In France and the plains of Germany ihe
average varies from 35 to 20 inches, but in mounts iric^u?
regions these figures are greatly exceeded, rising t!i rough
all gradations to upwards of 100 inches at some poiiits in
the Alps.
An important distinction between the manner of distri-
bution of the rainfall in the west of Europe and at mora
inland places is that the greater part of the annual quantity
of the west falls in winter, whilst in the interior the
amount in summer is greater than in winter. The rainfall
of January and July shows this in a very forcible
manner. The summer climates of the extreme south
of Europe and North Africa are rainless, and over exten-
sive regions in the south of Europe adjoining the July
rainfall does not amount to an inch. Over these dry
regions the prevailing winds of summer are northerly, and
hence the drought which characterizes thom. On the other
hand, the rainfall in the interior of the continent is large.
In January the maximum rainfalf occm-s on the mountains
and high grounds overlooking the Atlantic, and the
minimum on the plains of Russia.
Owing to the way in which Europe is broken up by the
seas which diversify its surface, the time of the year when
the rain attains the maximum differs greatly in different
regions. This phase of the rainfall occurs, indeed, accord-
ing to locality, in aU months except February, March, and
April. The month of occurrence of the annual maximum
rainfall over Em ope is shown by fig. 18. A similar map
Fia. 1,8.— Showing Jlonth of Ma
Rainfall in Europe.
representing tho month of least rainfall shows still greater
uniformity in a regular succession of the months in passing
from region to region. Thus tho month of least rainfall is
January on tho lower Volga, February in western Russia and
tho greater part of central Europe, March in the north of
France and south of Great Britain, April farther to the north.
BAINFALL.J
METEOROLOGY
May in Scotland north of the Grampians, June in Orkney,
Bhetland, Iceland, the west of Ireland, and the nonh-west
of France, and July over the whole of the south of Europe.
The driest month occurs nowhere in Europe in any of the
five months from August to December.
Eainfall of Korth America. — West of the Rocky Monntains the
rainfall is very unequally distributed, the annual amounts varying
from 86 inches at Astoria, near the monlh of the Columbia river,
to 8 inches at Sau Diego on the coast, and 3 inches at the head of
the Gulf of California. Qver the whole of the region between the
Cascade and Rocky Mountains the rainfall at all seasons is extremely
email, this being indeed that feature in the climate to which tha
fonnation of the canons of that region is chiefly to be referred. On
the other hand, in the United States and Canada to east of long. 100°
W. the distinguishing feature of the rainfall is the comparative
equableness of its distribution, an annual rainfall exceeding 50
inches occurring only over restricted districts, and a rainfall as low
OS 20 inches being scarcely met with anywhere. The regions where
the rainfall exceeds 50 inches aro Florida, the lower basin of the
Mississippi, and the Atlantic seaboards of Nova Scotia and Hew-
foundlana.
In January the annual maximum rainfall occurs over the whole
of the west coast from Sitka to lower California; but in the
Interior between long. 120° and 95° W. the amount is everywhere
email, and over a considerable part in the south-west of this region
no rain falls. The region of largest rainfall extends from Louisiana
to West Virginia, where the mean varies from 4 to 6 inches. Over
nearly tha whole of the Dominion of Canada, by much the greater
part of the winter precipitation is in the form of snow, which has
been carefully measured and recorded by tlic Meteorological Ser-
vice. The average snowfall for January exceeds 30. inches at St
John's, Newfoundland, in Anticosti, Piinca Edward Island, and
in many other regions.
In July the rainfall is everywhere small in the west, a large
part of this extensive region being absolutely rainless. The
remarkable dryness of the climate at this season is due to the N.W.
winds that set in towards the low pre3sur:> of the interior, which
thus blow towards warmer regions. The rainfall to the east of the
lEocky Mountains is distributed by the winds which are connected
iwith the low-pressure region of the interior and with the high-
jjressure region of the Atlantic. The result is two regions of larger
^nfall, the one in the south-east of the States and the other to the
rwest of the lakes. The summer winds of the south-eastern coasts are
■ontherly, and as they are anticyclonic in their origin and have in
their course traversed some extent of ocean, they arrive well- but not
super-saturated, and pour down a rainfall in July of 6 inchea and
npwarda along the coasts and for some distance inland from Louisi-
ana to Chesapeake Bay. Further, since in July these winds attain
itheir maximum force and persistency, the rainfall at the same
Itime reaches the maximum along the whole coast from Boston to
some distance west of New Orleans. Since the summer winds blow
in th"j line of the Alleghaay mountains and not across them, the
rainfall diminishes in ascending their slopes. The comparative
equableness of the rainfall over the eastern States is the necessary
Jesuit of the winds' passing into higher latitudes, and, therefore,
cooler regions. A broad region where the rainfall is less than on
each side of it, extends from Michigan to the south-west as far as
Canadian River. To the west of the lakes the rainfall rises above
4 inches, and, since over this region the winds become somewhat
easterly as they flow towards the low-pressure area, it is probable
that the larger rainfall of this prairie region has its origin in no
email degree in the evaporation of the lakes. On ascending the
higher reaches of the Mississippi, the amount diminishes, but
scarcely falls lower than 2 inches, being thus analogous to the
surn-.r.er rains of the Upper Gauges. On crossing the water-parting
into the basin wliich drams into Hudson Bay, we encounter E. and
N.K win Is laden with vapour licked up in their passage over Hud-
son's Bay, which they distribute in a generous rainfall of probably
5 to 6 inches over the rising colonies of Manitoba and Saskat-
chewan. An important point in the climute of the States is that
over nearly the whole of the extensive i-egion stretching between
Alleghanies and Rocky Mountains, except the south coast already
referred to, the annual maximum rainfall does not occur in summer
iut in spring, the month of largest rainfall in the great majority
of cases being Hay. In the basin of Hudson's Bay July is the
■month of largest rainfall.
Eainfall of Central and South Arwrica. — The following arc, in
Inches, the larger and more interesting annual rainfalls round the
coasts:— Vera Cruz, 182; Belize, 75; Maracaibo, 103; Caracas,
il65; Georgetown, 95; Paramaribo, 142; Cayenne, 140; Para, 71;
Teniambuco, 109; Buenos Ayrcs, 34; Bahia Blanca, 19; Puerto
MoDtt, 102; Valdivia, 109; Valparaiso, 100; Serena, 93; Lima,
8 ;^nd a large part of Peru, nil A remarkable feature of the
rainfall of South America is the large amounts that fall ill the
Insins of the Orinoco and Amazon: the Call is 91 inches in the
l(>— 8»
153
npper basin^of the Madeira, and 112 inches at Tijuitcs (lat. 3" 40'
S. , long. 72° 57' W.). The reason is that tliia immense regioa,
where pressurg appears to be almost constantly low, is open to tha
highly saturateu winds that blow from the equatorial Atlantic.
Quite different is the distribution of the rainfall over the La
Plata bpsin. The annual falls, in inches, are 92 at Joinville, 58
at Corrientes, 44 at Monte Video, S6 at Parana, 24 at Santiago,
22 at San Luis, and only 6 at Mcndoza. The fall rapidly rises in
ascending the eastern slopes of the Brazil mountains facing the
South Atlantic ; thus, while the amount at Rio Janeiio is 45
inches, on the hills to northward it is 116 inches.
In January northerly winds pre Jiil on the smith coasts of the
Gulf of Mexico and the. Cj-ibbean Sea, and as they have their
origin in the high pressure of the American continent, and in
crossing the sea pass into lower latitudes, the January rainfall of
these coasts is comparatively small. In July, however, the prevail-
ing winds are easterly, and as they have traverfi \ t. \irffe extent of
the equatorial waters of the Atlantic they ars higl.j^- saturated,
and consequently the July rainfall of these coasts is everywhere
very large. The following are, ill inches, the January and July
rainfalls :— Caracas, 1-00 and 14-04; Gnatemah, 0-2S and 10-79;
Vera Cruz, 5-10 and 35-90. The seasonal distribution of the
rainfall in the basin of the Amazon is the reverse of this. In
January the position of the belt of calms is about lat. 3° N., and
as pressure is rektively low over the basin of the Amazon,
especially its southrin slopes, the trades and the west portion of
the region of cabns anitcdly spread their highly saturated air over
the whole region as far as the Andes, resulting in one of the most
widespread heavy lainfaUs anywhere to be met with. On the
other baud, since in July the belt of calms is about lat. 10° N.,
the saturated atmosphere of the tropical regions no'longer flows up
the Amazon, but is caiTied westward into the Caribbean Seaand Gulf
of Mexico. Hence at this season the rainfall of the Amazon valley
is smalL The following are, in inches, the January aud July
falls:— Para, 6-51 and 3-26; Manaos, 7-33 and 1-82; ujiper
Madeira, 15-90 and 030 ; and Yquitos, 10-24 and 4-26. Ou the
La Plata in January pressure is low, and as ^vinds consequently
blow from the ocean in upon the region of low pressure the rainfall
is large ; but as pressure is high in the interim in July the i-aiufall
in that month is small. The following are, in inches, the Jannary
and July rainfalls :— Buenos Ayrcs, 2-37 aud 1-70; Parana, 4-63
and 1-32; Corrientes, 5 24 and 2-67; Joinville, 14-26 aud 3-55;
and San Luis, 2-63 and 0-00.
Rainfall of Africa. — As regards the i-ainfall, Africa presents the
greatest diversity in its climates. The following aro the annual
amounts in inches at various points ou or near the coast : — Port
Said, 2; Alexandria, 8; Tunis, 12; Algiers 31; Oran, 17; Mogador,
50; month of the Senegal, 17; Goree, 21; Sierra Leone, 126;
Christiansborg, 23; St Thomas, 40; Gaboon, 106; Loanda, 11;
Capo Town, 23; Mossel Bay, 12; Port Elizabeth, 24; Durban, 43;
Zanzibar, 68; and mouth of the Zambezi, 61. In the north of the
continent, the rainfall rapidly diminishes inland, and over the gi-cat
desert of Sahara practically none falls. In the iutericr of Algiers
it diminishes, the amount at Laghouat being 17 inches, and at
Biskra 9. In Egypt the rainfall is limited to a narrow strip along
the coast ; at Cairo the annual fall scarcely amounts to an inch.
The January and July rainfalls are, in inches, as foDows ; — Port
Said, 0-46 and 000; Alexandria, 1-95 and 0-20; Algiei-s, 4-43 and
0-04; Eiskra, 0-56 and 0-03; St Louis (Senegal), 0-23 -and 3 00;
Goree, 0-00 and 4-06; Sierra Leone, 069 and 24 20; Christiansborg,
0-50 and 2-00; Katunga, Oil and 4-76; Gaboop, 9 35 and 0-48;
Cape Town, 028 and 3-83; Durban, 5 00 and 170; Pretoria, 6-07
and 0-71; and Zanzibar, 2-02 and 2-35. At ZaUEibar the heaviest
rains occur about the equinoxes, the mean for April being 14-55
inches, and for October 6-80 inches.
In the case of this, as the other continents, the explanation of tno
different amounts is to be had in the seasonal changes of wind. In
the north the -winter rains are to a very large extent Ihe accom-
paniment of the Mediterranean storms of that season, but in summer
pressure is diminished in the interior and increased in the Atlantic
to the north-v.-st, resulting in strong steady northerly winds, wl.iu
as they advance iuto hotter regions are nnaccompanieiV xi-ii rain.
The heavy summer rains from Senerambia to the Gold Coast aro
due to the strong monsoonal winds which set in towards the
interior, thus dra-wing over these coasts the highly saturated air of
the belt of calms and of tlie trades immediately to the north and
south of it. Since in winter the belt of calms is removed 8 of
latitude farther to the south, and the temperature of the interior is
greatly reduced, it follows that the winds blowing on these co^ta
from the sea are drier and less strong, and consequently the rainfall
is small. At Sierre Leone the absolutely driest month is February,
0-31 inch, and the wettest September, 29-15 inches. On the other
hand, at Gaboon (lat. 0° 25' N.) the dry se.ison is from June to
August, when the belt of calms is farthest to the north ; and the
absolutely rainiest about the equinoxes, the mean of March being
14-70 inches and October 19-52 inches. At Loanda (l.-rt. 8 49 S.-)
the annual amount is only a tenth of what falls at Galioan, and it
154
METEOROLOGY
[snow.
falls wholly during the summer months of the southern hemisphere.
In South Africa pressure iji January is lowest in the inteiior,
towards which prevailing winds from the ocean blow, and as these
advance into regions becoming rapidly hotter the rainfall all round
the coast and for some distance inland falls to the annual minimum.
But in more sti'ictJy inland districts which arc at a considerable
elevation the rainfall reaches the maximum at the same season.
Thus the amounts in inch£s for January and July are — for Pretoria,
0-67 and 071; Maritzburg, 4'23 and 0-2]; Graham's Town, 2-89
and 1-51; Lower Nel's Poort, 1-33 and 0-49; and Aliwal North,
l'35and O'OO. In the winter months pressure in the interior is
high, and the rainfall consequently small. Though on the coast
winds from the arid interior frequently prevail, yet the storms that
sweep enstward past South Africa precipitate over large portions of
the southern slopes of this part of the globe what must in the main
be regarded as a generous rainfall. It follows that the climates of
these important colonies range themselves into two perfectly dis-
tinct classes, — the climates of the inland regions and the Natal
coast, where the rains occur during the hottest months, and the
climates of the other regions, where the annual rains occur during
the coldest months. Little is accurately known regarding the rain-
fall of the interior of Africa. It is certain, however, that it is
small, or nil, over the extensive region of the Sahara, and that it
is large from about 15° N. lat. to some distance south of the
equator. Probably the rainiest part of Africa is the region extend-
ing from the Victoria Nyanza northwards to and including the
gathering grounds of the tivo great tributaries of the Nile.
Snow. — Snow takes the place of rain when the tempera-
ture is sufficiently low to freeze the condensed moisture in
the atmosphere. Snow is composed of crystals, either six-
pointed stars or hexagonal plates, which exhibit the
greatest variety of beautiful forms, one thousand dif-
ferent kinds having been observed. These numerous forms
Scoresby reduced to five principal varieties : — (1) thin
plates, comprising several hundred forms of the most ex-
quisite beauty ; (2) a nucleus or plane figure, studded with
needle-shaped crystals; (3) six-sided, more rarely three-sided,
crystals ; (4) pyramids of six sides ; (5) prismatic crystals,
having at the ends and midille thin plates perpendicular
to theii' length. In the same snowfall the forms of the
crystals are generaUy similar. The flakes vary from 0'07
inch to an inch in diameter, the smallest occurring with
low temperatures and the largest when the temperature
approaches 32°. If the temperature is a little higher, the
snow-flakes are partially thawed in falling tlirough.it, and
ffail as sleet. The white colom' of snow is caused by the
combination of the difi'erent prismatic colom-s of the minute
snow-crystals. The density of snow is far from uniform ;
it L<i generally from ten to twelve times Lighter than an
equal bulk of water, but varies from eight to sixteen
times lighter than water.
The Umit of .the fall of snow near sea-level coincides
roughly with the winter isothermal of 52°, since in places
'where the mean winter temperature -is no higher than 52°
that of the air falls occasionally to 32° or lower during the
winter months. As regards Em-ope, the southern limit is
about Gil'raltar; in North America it is Savannah, New
Orleans, tLe mouth of the Rio Grande, the head of the Gulf
iof California, and San Francisco. In Europe, north of lat.
60°, snow falls generally on an average of from 80 to 110
days in the year. At Upsala the number of days is CI,
at Warsaw 45, Aberdeen 42, Oxford IS, Ostend 15, Brus-
sels 27, Tarum (in the south-west of Jutland) 12, Copen-
hagen 23, Vienna 33, Odessa 19, Sebastopol 12, Milan.
11, ■ Trieste G, Saragossa 5, Madrid 3, and Lisbon 1.
In Greenland the nUinber of days exceeds 80, and this
figure is nearly reached in Newfoundland and the north-
east seaboard of Nova Scotia. At Quebec the mean days
of snow are 66, Halifax 64, Winnipeg 04, Detroit 34,
Cape Henry 13, St Louis 11, mouth of the Columbia
River 7, and Charleston 2. In Russia the time of the
year when snow falls most frequently is December and
January, except in the south of the empire, where February
is the month of the most frequent occurrence of snow.
But to the north of a lino drawn from the entrance o£_the
Gulf of Finland through Warsaw, Cracow, Salzburg, and
Santiago March is the month of maximum occurrence in
the great majority of instances ; while to the south of this
line it is January and in several cases December.
The largest falls of snow occur in the Antarctic regions,
as is well attested by the magnificent icebergs of solidified
snow which break off all round from the lofty walls of ice
that engirdle the Southern Ocean. Excepting perhaps in the
Dominion of Canada, no data have been anywhere collected
from which even a rough estimate could be formed as to
the mean annual amount of snow that falls in different
parts of the globe.
Snow-Line. — The snow-line marks the height below
which all the snow that falls annually melts during summer.
No general rule can be stated for this height in different
climates owing to the many causes determining it. Thesa
are the exposure of mountain slope to the sun (and hence,
other things being the same, it is higher on the south than
on the north sides of mountains), exposure to the rain-
bringing winds, tlie steepness of the mountains, and the
degree of dryness of the air. Hence the position of the
snow-line can be known by observation only. It falls only,
little on either side of the equator to lat. 20° ; from lat.'
20° to 70° it falls equably, but from lat. 70° to 78° mucW
more rapidly. To this general rule there are many excep-
tions. It IS 4000 feet higher on the north than the soutt
side of the Himalayas, owing to the larger snowfall on the
south, and the greater dryness of the climate of the north
side, and therefore the greater evaporation from the snow
there. It is higher in the interior of continents than near
the coasts, because the precipitation is less and summer heat
greater. In the Caucasus it is 11,063 feet high, but ordy
8950 in the Pyrenees. In South America it rises from the
equator to lat. 18°, and more on the west than on the east
slopes of the Cordilleras, owing to the large precipitation or.
the east and small precipitation and arid climate of the west
side of that chain of mountains. It is as high in lat. 33'
S. as in 19° N., but south of that latitude it rapidly sinks
owing to the heavy rains brought by the moist N.W.
winds of these regions. In the south of Chili it is 3000
feet lower than in the same latitudes in Europe, and 6000
feet lower than in the extremely arid climates of the Rocky
Mountains.
Storms. — If weather charts representing a large part of
the northern hemisphere be examined, two distinct systems
of pressure are seen which change their forms and positions
on the earth's surface from day to day. The one set are
systems of low pressure marked off by concentric isobars
enclosing pressures successively lower till the centre is
approached ; and the other systems of. high pressure
marked oS by concentric isobars enclosing pressures becom-
ing successively higher towards the centre. The former of
these are called cyclones, and the latter anticyclones. These
areas of low pressure are the distinguisliing 'characteristic^
of the hurricanes and typhoons of tropical regions, and of
the ordinary storms of lugher latitudes, and they may all
be conveniently grouped under the general name of cyclones.
Fig. 19 shows a storm which was passing across north-
western Europe on the morning of November 2, 1863, and
it may be taken as fairly representing the general features
of cyclones. In the figure the arrows fly with the wind,
and tlie force of the wind is indicated by the number of
feathers on the arrows.
It will bo seen that the winds indicate, not a circular
movement round the centre of lowest pressure, but eC
vorticose motion inwards upon that centre, the motion
being opposite to that of watch-hands. In other word.>>,
the wind follows Buys Ballot's law, already explained.
The winds are strongest where the isobars are closest
together ; or they are generally proportioned to the " baro-
STORMS.]
METEOROLOGY
155
memo gradient," — a term introduced by Stevenson in
1867. Cyclones have diameters seldom less than 600, and
they occasionally exceed 3000 miles; the cyclone of fig. 19
had a diameter of about 1-200 miles. The cyclones of
the Mediterranean are
usually of smaller dimen-
sions than those of north-
western Europe and
America. The rates at
which cyclones advance
over the earth's surface
vary greatly, the average
in America being 24
miles an hour, in the
Atlantic 20 miles, and
In Europe 26 miles. A
rate as high as 70 miles
an hour has occurred in
the British Islands ;
sometimes they remain
stationary, and more
rarely their course is
for a time retrograde.
The temperature and ^^' ''
humidity increase at those places towards and over which
the front part of the storm is advancing, and fall at those
places over which the front part of tlie storm has already
passed. In other words, the temperature and humidity
rise as pressure falls and fall as pressure rises. This is
the important climatic significance of cyclones. Thus a
succession of low pressures passing eastwards in courses
lying to northward of the British Islands are the essential
ooaditioua of open winters ; whereas, if the cyclones follow
courses lying to southward, the winters are severe. In a
cyclone the broadest feature of weather is an area of rain
about or rather somewhat in front of the centre, sur-
rounded by a ring of cloud, outside which the sky is clear.
The precise form . and position of these areas have been
shown by Abercrombie to vary ^vith the type of pres-
sure distribution, with the intensity of the cyclone, and
ivith the rate of its progress, and they are also influenced
by local, diurnal, and seasonal variations.
The chief point of difference between Ajnerican and
European storms is essentially the result of the mean
winter pressures to the west and north-west of their respec-
tive storm-tracks. Owing to the high ^vinter pressure m
the interior of America, the barometer rises in the wake of
:he storms of the United States more rapidly, the wind
reers round more quickly and more uniformly to N.W.,
N.N.W., and N. and keeps longer in these directions,
ind the temperature and humidity fall to a greater
degree, than happens in Europe. In the New England
States and Canada the easterly winds of the storms,
.'oming as they do from the Atlantic, are disagreeably
:old, damp, and misty in a degree and with a frequency
iiuch greater than occurs with the same winds in the
-British Islands.
The chief points of difference between the hurricanes and
typhoons of the tropics and the cyclones of higher latitudes
are these : — tropical cyclones are of smaller dimensions,
show steeper barometric gradients and therefore stronger
winds, and advance at a slower rate over the earth's
surface. Another point of difference is that a large number
of the hurricanes of the West Indies and the typhoons of
eastern Asia first pursue a westerly course, which gradually
becomes north-westerly, and on arriving at about lat. 30°
they recurve and thereafter pursue a course to north-east-
wards. The tropical cyclones of the Indian Ocean south
of"the equator also first pursue a westerly course, which
gradually changes to south-west, and often on arriving about
lat. 30° recurve to the south-east. Many of the cyclones of
India have their origin to westv>-ards of the Nicobar Islands,'
pursue a course to north-westward, and die out in the
valley of the Ganges ; and, similarly, a considerable number
of the cyclones of the West Indies pursue a westerly course
through the Gulf of Mexico, and several die out in the States.
The most dreadful attendant on tropical cyclones is
the storm-wave, caused by the in-bl^owing winds and the
low pressure of the centre of the storm. When this wave
is unusually high and is hurled forward on a low-lying
coast at high water it becomes one of the most destructive
agents known. The Bakarganj cyclone of October 31,
1876, was accompanied by a wave which flooded the low
grounds to the east of the delta of the Ganges to heights
varying from 10 to 45 feet, by which more than 100,000
human beings perished.
Trachi of Cyclones of North America, Atlantic, c/ttd
Europe. — In the Physical Atlas of tlie Atlantic Ocean, issued
under the direction of Dr Neumayer of the Deutsche
Soewarte, plate 28 shows by shadings the mean positions of
the centres of cyclones and by lines their mean tracks.
The follo\ving are the regions where the lowest barometer
of storms has been most frequently found: — the region;
to west-south-west of the lakes of the United States ; the
Gulf of St Lawrence ; mid- Atlantic about lat. 35° long. 52° ;
to the south-west of Greenland; to the south-west of Iceland,
which is by far the most important of the whole ; to the
south-west of the Lofoten Isles; the region embracing
Denmark, the south of Scandinavia, and Finland : and, as
secondary centres of frequency, the south of the British
Islands, Corsica and part of Italy adjoining, and the north-
east of the Adriatic. The great importance of these centres,'
where the lowest barometers are most frequently found,
consists in the indication they give of the precise regions
either where many storms originate or where they are
either retarded or arrested in their course. As regards the
origin of storms, the centre west of the Mississippi is the
region where most of the United States storms originate,
the centre in "the Gulf of St Lawrence is where many of the
great Atlantic storms have their origin, and the centres in
mid-Atlantic and to the south-west of Iceland are the
regions where the storms of north-western Europe chiefly
originate. The centres on the south-west of Greenland,
the Lofoten Isles, Denmark, and the south of the British
Islands, all appear to suggest that storms are retarded in
their onward courses on coming up against large masses of
land, — which may, in part at least, be occasioned by the
heavy rainfalls that mark these parts of their courses.
Of all storm tracks the most frequently taken is that by
the storms of the United States, which pursue an easterly
course through the lakes to the Gulf of St Lawrence. A
considerable number of storms follow a course from Nova
Scotia to Davis Straits ; but the larger number take a
north-easterly course through the Atlantic towards Iceland
and thence past the north of Norway. Among the less
frequent but important tracks are these : — from near Newi
Orleans along the east coast of the States towards Nova
Scotia ; from mid-Atlantic to south of Ireland and thence
through France to the north of the Mediterranean; and
from the Atlantic about kt. 42° long. 40° in a north-
easterly course quite outside but at no great distance from
the British Islands, and thence towards the North Cape.'
Of the tracks more immediately affecting British weather
are one from Iceland in a south-easterly direction through
the North Sea and Germany, and four tracks which start
from near Scilly: — (1) to the south-east as already described;
(2) eastward through the north of Germany ; (3) north-east
to Christiania ; and (4) north through Ireland and the
Hebrides. These are the storm tracks which chiefly give,
the United Kingdom its easterly and northerly winds. ,
156
METEOROLOGY
The Inclination of Winds to ilie Isobars. — Tho vorticose
motion of the wi-.id in a cyclone towards and in upon the
ceutre has been already pointed out. One of the more
important practical problems of meteorology is the dtter-
mina'ion of the angle of inclination of the ■ninds to the
isobars in the different segments of the cyclone, not only
from the application of the results of the inquiry to the
theory of storms but also to practical navigation. The first
real contribution to the subject, based on accurate measure-
ments, was made by Clement Ley in 1873.' From the
observations made at fifteen places in north-west Europe
examined by him. he showed that the winds incline from
iiistricts of higher towards those of lower pressure at a
mean angle of 20° 01'; that the incliuatiou is much greater
at inland than at well-exposed stations on the coast, the
respective angles being 28° 53' and 12° 49' ; and that the
greatest inclinations are with S.E. winds. Then follow
S.W., N.E., and N.W. winds, the last showing the least
inclination. Whipple has recently compared the winds
at Kew with the barometric gradients for the five years
ending 1879, with the result that the greatest inclination
lis 63° with S.E. winds, the least 35° with N.E. winds, and
the mean for aU winds 52°.
As regards the open sea, Captain Toynbee has shown,
(from a careful investigation of the gi-eat Atlantic storm of
I August 24, 1873, that the mean angle of inclination
calculated from one hundred and eight observations was
29°, the mean at the three selected epochs examined
'varying from 25° to 31°.
Barometric Gradient and Velocity of the Wind. — In
.inquiring into the relation of the velocity of the wind to
the barometric gradient, it is necessary to have some
definite information as to the increase of the velocity with
'height above the" ground. Stevenson recently made
observations on this point on winds varying from 2 to 44
'miles an hour from the sm-face up to a height of 50 feet,
from which he has drawn the following conclusions : — (1)
the spaces passed over in the same time by the wind
increase with height above the ground ; (2) the curves
traced out by these variations of velocity from 13 to 50
ieet high coincide most nearly with parabolas (fig. 20)
/»//
iW
having their vertices in a horizontal lino 72 feet below the
surface ; (3) between 15 feet and the ground there is great
disturbance of the currents, so that the symmetry of the
curves is destroyed ; (4) the parameters of these parabolas
increase directly in tho ratio of the squares of the velocities
of tho different gales. If x be the velocity of the wind
' Journal Scottish Meteorological Sociel;/, voL iv. p. 63.
ivrara veloctit.
at height II above the ground, fho parameter of tho
corresponding pai-abola is ^-/(n + '!'2j : and an x varies th»
parameter will vary as x- or as the square of the velocity
of the gale. It follows that, to render wind observations
comparable, it is necessary that anemometers be placed at
one uniform height above the ground, and that standard
height not lower than 15 feet above the surface. It is
very desirable that tho inquiry were prosecuted Uj) It; a
height of 100 feet ; and it is of the utmost importance that
the variation in the diurnal velocity be at the same lime
determined at different heights from 15 feet upwards.
Stevenson olso made wind observations on the Caltoa
Hill, Ai-thui's Seat, and the Pentland Hills, in the vicinity
of Edinburgh, up to a height of 1600 feet above sea-leveL
It is from observations made at stations on knolLs and
peaks at different heights above the sea, and at different
heights above the surfaces of their summits, that the
problem of the variation of the wind's velocity at different
heights with the same barometric gradient can bo ascer-
tained. In carrying the inquiry to considerable heights,'
the results cease to be comparable with those obtained
at lower levels, unless in those cases where neighbouring
heights are available for data from which the barometric
gradient at the observed height can be calcidated. The
results of observations as to the velocity of atmospheric
currents at very great elevations in the atmosphere deduced
from the apparent movements of the higher clouds are
altogether incomparable with the winds near the surface of
the earth, for these among other reasons : — the heights of
the clouds can be at best but imperfectly ascertained; the
motion of the clouds, "particularly the higher clouds, may
be only apparent, it being sometimes difficult to distinguish
between the formation and dissolution of clouds and their
motion ; and above all, since the higher clouds are usually^
the accompaniments of the greater weather changes, their
movements are the result of barometric gradients towards
a knowledge of which we are absolutely powerless to take
a single step.
As regards surface winds, Clement Ley in 1881, and
Whipple more recently and with greater fulness, have
calculated the mean wind velocities for twelve gradients, — ■,
the gradients being derived from the daily weather charts
of the Meteorological Office for the five years 1875 to 1879
at 8 A.M., and the corresponding wind data being obtained
from the hourly readings of the Kew anemograph. Thej
barometric gradient is for 15 nautical miles, and tho
following are the velocities for the twelve gradients on the
mean of the year: —
Gradient.
Velocity.
Gradient.
Velocit
0 002
6-0
0 017
15-0
0 005
7 0
0-020
JG-5
0 007
7-5
0-022
19-1
0010
9-2
0-025
22 0
0-012
11-6
0-027
22-0
0-015
12-6
0-030
25-5
The influence of season is very strongly marked. The
velocities for the same gradients in order are — October to
December, 125 miles; July to September, 12-6 miles;
January to ilarch, 148 miles; and April to June, 17-2
miles. From those observations of Whipple it follows
that during the six months -when the temperature is falling
the velocity for the same gradients is least, while the velocity
is greatest during the six months when tho temjierature is
rising, and absolutely greatest during tho three months
ending Juno, when tho greater part of the annual increase
of temperature occurs. It is evident that the observed
increase in the velocity of tho wind for the same gradients
is to be referred to tho same cause that brings abort the
diurnal increase in tho wind's velocity, viz., the wind
blowing over a warmer surface than itself.
WEATHER ?.tA?3.]
METEOROLOGY
157
Whipple has nlso sorted the -winds according to the
eight points of the compass, with results of the greatest
inUrest. If N.W., N., N.E., and E. winds be grouped
together as polar, and S.E.,. S., S.W., and W. winds as
equatorial winds, the mean hourly velocity of the polar
winds, for the same gradients, is 1-1 miles in excess of the
equatorial winds. Now, since polar winds pass into lower
latitudes, the surface of the earth over which they blow
is warmer, whereas the surface is colder than the equa-
torial winds which blow over it. It follows that the
increased velocity of polar winds is referable to the same
conditions which result in the diurnal increase in the
•wind's velocity and the greater velocity for the same
gradients of winds when the annual temperature is rising,
since in all these cases the winds blow over a surface of
a higher temperature than their own.
It is evident from these considerations that for the
development of the law of the relation of the wind's
velocity to the barometric gradient ^^•ith an exactness
sufficient to warrant us in expressing that relation in a
general mathematical formula much yet remains to be done.
In truth, as regards the various formulae submitted by
Ferrel, Mohn, Hann, Everett, and others, we have no
choice but to allow the justness of Strachan's criticism
(Modem Meteorohf/y, p. 98) that the theoretical values
furnished by the formulae do not accord with the actual
values, and that therefore a satisfactory formula is yet to
be found. Ere such a formula need be looked for, the
conditions must be fulfilled for the preliminary work of sup-
plying the observational data required. The "Challenger"
observations prove that, nith gradients substantially the
game, the velocity of the wind is greater on the open sea
than near land ; and we have seen that the velocity varies
with the hour of the day, and generally is increased as the
temperature of the surface rises above that of the air blow-
ing over it, and diminished as the temperature of the surface
falls below that of the air. It is evident that observations
on the open sea wUl afford data for the simplest solution of
the problem ; but on land the diurnal, seasonal, and non-
periodic changes of temperature greatly complicate the
problem, and render necessary for its solution observations
specially designed for the purpose. It is not easy to see
how these can be obtained but by carrying out the plan pro-
posed in 1875 by Stevenson of establishing strings of well-
equipjied meteorological stations planted sufficiently close
that the barometric gradients may be determined \\-ithin the
limits of accuracy required. Observations made twelve
times daily for a year, at stations so arranged, would
supply the observational data for the solution of this funda-
mental problem in meteorology. Till some such proposal
be carried out, the problem remains unsolved, for barometric
gradients lased on the \ridely separated existing stations
are too uncertain and rough and the wind observations
«re wanting in that comparability which alone can satfef^
the inquiry.
Weather and VTialher Maps. — Weather is the state of
the air at any time as respects heat, moisture, Txind, rain,
cloud, and electricity; and a change of weather implies a
change in one or more of these conditions. Of these
changes the most important as regards human interests
are those which refer to temperature, wind, and rain; sid,
as these are intimately bound up ^ith the distribution of
atmospheric pressure, the latter truly furnishes the key to
weather changes.
These rrl.itions arc well shown by the Intfmationnl Jfontlily
Weatlicr JLips is.suoa liy the UniteJ States Signa] Service. Of these
lh.it for Decciiibcr 1878 is a strikiiifr example. This month nns
ehnncterizcd over the {jlobe by imusually abnormal weatlicr. A
Knc drawn from Texas to NewfounJl.anU, across the Atlantic, the
.Aocth of France, ami Ocrniany, thence round to sonth-east, through
"tUi Black Sea, the Cauca:>U8, luJia, th« East ludia Islands, and
Anstnlia to the South Island of New Zealand, passes through i
broad and extended region where pressure was throughout con-
siderably below the mean of December, and this low pressuro
was still further deepened in various regions along the line. An-
other line pa-ssing from Australia, through the Philippine Islands,
Japan, tianchuria, Behring's Strait, and Alaska, also marks out
an extensive region \yhere pressure was uninterruptedly below the
mean.
On the other hand^pressure was above the average, and generally
largely so, over the United States to west of longitude 90°, over
Greenland, Iceland, the Faroes, Shetland, and a Targe portion of
the Old Continent bounded by a line drawn from Lapland round
by Lake Balkhash, Canton, Peking, to the upper reaches of the
Lena. Another area of high pressure extended from Syria, through
f;gypt and East Africa, to the Cape ; and part of n third area of
high pressure appeai-ed in the North Island of New Zealand. As
regards North America, the greatest excess of pressure, 0'196 inch
above the mean, occurred in the Columbia Valley, from which it
gradually fell on proceeding eastward to a defect from the averago
of 0'146 iuch near Lake Champlain and to northward, rising again
to near tlio mean on the north of Nova Scotia. To the north and
north-east exceedingly high pressures for these regions and the
season prevailed, being 0'635 iuch above the mean in Iceland,
0 •.500 in the south of Greenland, and at the three stations in "West
Greenland, proceeding northward, 0"415, 0^402, and 0-346 inch.
AVest Greenland being thus on the west side of the region of
high pressure which occupied the noi-thern part of the Atlantic,
and on the north-east side of the area of low pressure in the States
and Canada, strong south winds set in over that co.-ist, and the
temperature at the four Creenl.ind stations, proceeding from south
to north, rose to 1°-1, 8°-8, 12°-1, and li°i above the means. As
the centre of lowest pressiire was in the valley of the St Laivrence
about Jlontreal, strong northerly and westerly winds predo^iinated
to westward and southward, where consequently temperature was
below the average, the deficiency at Chicago and St Louis being
9'*5; and, winds being easterly ami northerly in California, the tem-
perature tliere was also under the mean. On the other hand, in the
New England Spates, the greater part of the Dominion of Canada, and
"West Greenland tcmiierature was above the averago. Pressure was
much hi;;hcr at St Slichael's, Alaska, than to south-westward at St
Paul's, Behring's Strait, and hence, while temperature at St Paul's
w-as 2°*9 below the normal, it was 12" -0 above it at St Slichael's,
where strongly southerly winds ruled. AVith these strong contrasts
of pressuiv, America presented contrasts at least as striking in the
distribution of the temperature. Along the south of Lake Alichigan
the November temperature was 13'^7 above the normal, whilst the
December temperature was 9*-5 below it, the difference there •
between the two consecutive months being thus 23''2.
As regards Europe, Iceland was on the east side of the patch of
high pressure which overspread the north of the Atlantic, and hence
northerly winds prevailed there and temperature fell 7°^2 beloT?the
mean, presenting thus a marked contrast to the high tcmperatut»
of West Greenland at the time. In Europe, the area of low-est
pressure occupied the southern shores of the North Sea, extending
thence, though in a less pronounced form, to south-eastward.
Hence over the whole of western Europe winds were N K., N., and
in the south-west of Europe W. ; and hence everyw ha-e from the
North Cape to the north of Italy temperature was below the
normal, in some places greatly so, the deficiency being 10""4 in
the south of Norway and 12°-2 in the south of Scotland. On the
other hand, on the east side of this area of low pressure winds were
southerly and temperature consequently high. In soine localities
in Russia the excess above the mean was 15"^0, and over a large
proportion of European Russia the excess was not less than 9*^0.
This remon of high temperature extended e.-istward into Siberia a.^
far as the Irtish, being coterminous with tlie western half of the
anticyclonic region of high pressure which overspread central
Siberia. But over the eastern portion of the anticyclone northerly
winds prevailed, witJi the inevitable accompaniment of low tem-
peratures over the whole of Eastern Asia, the deficiency at Ner-
tchinsk on the upper Amur being 6°^8. Here again, just as in
America, Greenland, and Iceland, places w-ith atmospheric pressure
enually high presented the strongest contrasts ot ftmperature.
TnusatBogoslovsk, on the Ural Mountains, pressure was 0211 inch
and at Nertcliinsk 0154 inch above the nonnals, but Bogoslovsk
on the west side of the high pressure area had a temperature 15°'0
above, whilst at Nerteliin>k it was 6°'$ below the average.
At this time of the year the mean pressure falls to the minimnm
in Australia, but during December 1878 the usually low pressure
was still furtlicr diminished. Pressure at this sc.ison also falls to
the annual minimum in the North Pacific and North Atlantic,
and it has been seen tliat the low pressure of these regions was
likewise still further diminished. But in the case of the Atlantic
it was attended irilh a most important difference. The centre of
lowest pressure, usually loc.itcd to the south-west of Iceland, was
removed some hundreils of miles to the south-east, and an unwonted
developmeat of extraordinarily high pressure appeared to the DOrtli*
158
M E T E O K O L O'G Y
[>vj;athee fokecasts.
iwarJ, overspreading the extensWe region of Baffin's Bay, Greenland,
Iceland, Faroes, and Shetland. It was to this region of high pres-
sure, particularly in its relations to the low-pressuro region to the
south-east of it, that the extreme severity of the weather in the
.British Islands at the time was due. Now this high-pressure
region was intimately connected ftith, and douhtless occasioned
directly by, upper atmospheric currents from the widely extended
region of low pressure to southward, with its large centres of still
lower pressure iu the North Sea, mid- Allan tic, and United States,
where pressures wel-e respectively 0-307, 0-322, and 0-146 inch under
the normals. Thus, with the single exception of the high-pressure
area about Greenland, the meteorological peculiarities which render
December 1878 so memorable over nearly the whole globe arose out
of a distribution of the earth's atmosphere essentially the same
that obtains at that time of tlie year, but the usu.il irregularities
in the distxibution of the pressure appeared in more pronounced
characters.
Taking the all-important bearings of these areas of high
and low pressure on -weather and climatelnto consideration,
along with the abnormal concentration of aqueous rapour
over extensive regions -which they imply, it is evident that,
-when the meteorologist will be in a position to forecast, on
scientific grounds, the weather of the coming season for
the British Islands, it is to the Atlantic he -will require to
look for the data on which the forecast is based.
These questions, which the International Weather Maps
of the United States enable us to discuss, are of the first
importance in meteorology, whether we consider the ampli-
jtude of the atmospheric changes they disclose (these being
often so vast as to embrace four continents at one time,
besides being profoundly interesting from their direct
bearings on the food supplies and commercial intercourse
of nations) or regard the larger problems they present,
-with hints towards their solution, which underlie physical
geography, climatology, and other branches of atmospheric
physics. The discussion -presents' the great atmospheric
changes as influenced by oceans and continents, including
the subordinate but important parts played by mountain
ranges, extensive plateaus, and physically well-defined
river basins in determining the development, course, and
• termination of these changes.
Weather Forecasts and Sionn Warnings. — It is in tropical
and subtropical countries that an isolated observer may,
with a close approximation to certainty, predict the
approach of gales and hurricanes. In these regions atmo-
spheric pressure and the other meteorological conditions
are so constant from day to day that any deviation, even
a slight one, from the average of the hour and season in
respect of pressure, the direction and strength of the -wind,
^and the direction and amount of cloud, implies the presence
of a storm at no great distance. Dr Meldrum has practically
iworked out this problem at Mauritius with great success.
'At the Royal Alfred Observatory there the mean pressure
at sea-level in January at 9 a.m. is 29'966 inches, from
Iwhich it falls to 29-904 inches at 4 p.m., then rises to
i29-980 inches at 10 p.m., and again falls to 29-927 at 4
'a.M: The mean direction of the wind and the diurnal varia-
tion, both as regards direction and force, have been stated
(p. 125). Suppose then that the barometer is observed
to fall after 9 a. si. more rapidly than is due to the usual
daily barometric tide, that in the afternoon it does not
indicate the second maximum or that it continues to fall
instead of rising, — or suppose, in short, any deviation from
the mean daily march, — then it is certain that there is
somewhere an atmospherical disturbance near enough to
Mauritius to influence- the pressure. The direction in
which the disturbance is from Mauritius is readily known
from the ■wind, and the distance of the storm closely
approximated to by noting the rate and amotint of the fall
of the liarometer, in connexion with the changes of the
-«'ind and the clouds, — the rate and progressive motion of
the storm being known chiefly from the veerings of the
wind. ■* For_a good many years past notifications Lave
been sent to the daily newspapfr^ when obscr<-ations show-
that a storm is not far from the island, stating its position
and probable course from day to day. The scheme of
storm warnings at Mauritius has been entirely successful,
and the result is of great value, since it shows what may be
done at an isolated station in the ocean, sr what may be
done in ships at sea. In this connexion it is not possible
to cverestimato the importance to seamen of a knowledge
of the hourly variations of the barometer and its mean
monthly heights over the ocean tracks of commerce.
In passing from Mauritius to the British Islands we
pass from a region where the forecasting of storms and
weather is simplest and easiest to the region where it is
most complex and difiicult, particularly for the western
districts of these islands. The great difTiculty lies in the
fact that the British Islands are immediately bounded by
the Atlantic to westwards ; and, since practically ever)'
storm and nearly all iveather changes come from that
direction, no telegraphic communication of their approach
can be received. The Meteorological Office in London has
therefore no choice but to base the forecasts on such of the
observations telegraphed to the office as experience has
shown to be the precursors of storms and other weather
changes. The more important of these observations are
the falling and rising of the barometer taken in connexion
-with changes in the direction and force of the wind. Since
on the north side of the track of the centre of the storm
winds are northerly and easterly and temperature low, and
on the south side winds are southerly and westerly and
temperature high, one of the most important points to be
ascertained is the probable path the centre of the coming
storm -will take. Though a good deal remains to be
accomplished in the development of this phase of storms,
yet much has recently been done in this direction by close
examination of the changes of pressure in the region of
the anticyclone contiguous to the advancing storm and by
the changing positions of the rain area near the centre of
the cyclone.
As fegards Europe, the facility of forecasting storms
increases as distance from the west coasts is increased.'
Thus to the middle and eastern districts of the British
Islands, were a day and night watch established in the
west, forecasts of almost every storm could be issued, the
exceptions being those small cyclones or satellite cyclones,
as they are called, originating -within the British Islands
themselves, which are frequently characterized at once bv
their severity and by the rapidity of their onward covirse.
In the United States, the system of -weather forecasting is
perhaps the best in temperate regions, — a result due tc
the admirable system organized and developed under the
direction of the late General Myer, and adequately sub-
sidized by the Government, but above all to the facilities
to detect and ti-ack the storms in the region where nearly
all of them have their origin, to west of the Mississippi,
before they advance upon the more thickly peopled States,
Meteorology sustained a heavy loss by the death in 1877
of Leverrier, who was not only the keenest-sighted of
physicists but also the prince of orgauizers of systems of
meteorological observation. His last great service to the
science was the establishment of a system of observation,
by which the propagation of rain, hail, and other weathei
phenomena could be followed and recotded from commune
to commune over France. This scheme for the investiga-
tion of the vitally important bearing on the meteorology
of a country of a comprehensive observation of its rainfall,
hail, and thunderstorms, through numerous observers
possessing sound local information, is not only eminently
just in science, but is calcidated to bo attended with tlie
greatest benefits to agricultural and other public interests.
The practical advantages of the scheme, it need scarcely
TIBKBSTKLAJ. MAGIiETISM. ]
METEOROLOGY
be added, can only be reaped after, a very large expendi-
ture of labour and money in organizing a comprehensive
parochial scheme of observation, systematically and per-
sistently carried through and discussed.
Further oetaila regarding meteorological phenomena
will be found in the articles Atmosphere, Babometer,
Climate, HyGEOMEXKy Ozone, Raingauge, Sea, and
Theemomeiek. (a. b.)
TEKRESTKUL ILiVGNETISM.
1. In the preceding portion of tin's article some account has been
ffiven of tlio influence which the sun and moon exeil upon the air,
the earth, and the ocean, their strictly tidal effects being left to be
separately dealt with. The discussion of the influenoo of these
bodies on what may be termed the movables of the earth will
not be complete, however, without embracing an account of the
changes which they produce in the earth's magnetism. An account
of the earlier magnetic observations has already been given under
the heading Magnetism, and our task will now be to give in the
first place a description of the best and most recent instruments by
which the magnetic state of the earth is determined, embracing
therein observatory iustiuments, those adapted for travellers whether
by land or by sea, and differential magnetometers. We shall next
give a short account of the magnetic system of the earth and of its
secular variation; and we shall then investigate the changes con-
nected with terrestrial magnetism depending ou the sun and moon.
In performing this task we shall be led to conclude that the sun's
power is variable, and we shall therefore examine whether this con-
clusion is likewise borne out by strictly meteorological observations.
Finally, we shall venture on remarks embodying a provisional
working hypothesis, and otu: object will bo gained if this should bo
found to suggest certain lines of thought to those interested in the
subject which may lead them to examine and discuss the very great
mass of observations at present existing.
iNSTEtTMENTS FOE DeTEEMININO THE M.\GNETIC St.^.TE
OF THE Earth.
(a) Observatory InstrXLmcnts.
2. Declinometer. — It is that end of tho needle which points to
the north magnetic pole of the earth of which the position is invari-
ably noted even when tho observation is made in the southern
hemisphere. The difference of this position from true geogi'aphical
north denotes what is called tho variation or declination (east or
west) of tho needle. East ia often reckoned negative and west
positive. The instrument by which this information is obtained is
called the declinometer. Tho unifilar magnetometer, which is
the form of declinometer now used, is described and figured in
Magnetism, vol. xv. p. 238.
3. ZHp Circle. — The instrument by which the magnetic dip or
iiieliuation is observed contains a thin needle about 3 inches
long, the centre of gravity of which coincides as accurately as
possible with the axis of motion of the needle. The needle has two
axlea consisting of two very fine cylinders of hard steel standing at
right angles to the plane of the needle, and great attention must be
paid to keep these axles in a state of perfect polish and dryness.
By means of these the needle can oscillate iieely on two horizontal
agate rounded edges, the one axle Ij-ing on the one edge 4nd the
other axle on the other. If the centre of gravity coincides exactly
with tho axil of motion, and if there be no adhesion or friction
between tho axles and the agate edges, the needle must settle into
such a position that its magnetic axis lies in the tiue line of dip.
The position of the ends of the needle is read by means of two
microscopes which move round on a cross piece carrying verniers.
Tp view the position of the lower end of the needle we move round
the lower microscope until the cross wire in its field of view (extend-
ing in the line between the two microscopes) symmetrically cuts
the extremity of the needle. The lower vernier is then read. Tho
same process is repeated for the upper vernier, and tho mean of
the two readings is taken. This mean wiU accurately denote the
position of the needle if the circle is properly set.
The sources of error in a dip observation are — (1) a want of
symmetry in mass, the centre of gravity of the needle not being
coincident with the axis of motion ; (2) the vertical circle being
erroneously set ; (8) a want of sj-mmetry in magnetism, tho mag-
netic axis not bemg coincident with the. axis of figure ; (4) excen-
tricity, the axis of rotation of the needle not passing through tho
centre of the circle ; (5) friction and adhesion of the axles as they
rest on their a^te supports. This last source of error is guarded
against by taking great care oi tho ixl^, and by inserting them
igently into a piece of cork before each observation j the agate
•upports ought also to be rubbed wjti cork. Then, again, when
!ih».n«:d]e has assumed its position, before reading ft is gently raised
jby means of s lifter, the handle ftr tur- eg which is shown in the
iSgnxe towitd.« tht right. It is then gently lowered, ard this pro.
169
cess is repeated until no apparent change of position is produced,
by the operation.
4. We shall now describe a complete dip observation. The first
point is to make the needle to swing in the plane of the magnetic
meridian. In order to accomplish this, after levelling the instru-
ment, the verniers are set for 90°, that is, for a vertic^ position of
the needle. The whole instrument is now turned round its hori-
zontal circle until the exti'emitios of the needle are bisected by the
wires of the two microscopes, and the positiou of tho vernier of tho
horizontal circle is then read. The needle is next reversed so that '
the microscope shall view its other fiat side ; it is made vtstical aa<
before, and tho position of the horizontal circle read once moi-e.
Ne.xt the face of the instrument is turned round 180°, and tho same
two operations repeated. We have thus fom- readings of the hori-
zontal circle, and if we take the mean of these we sliall have ascer-
tained with sufficient accuracy the position of that plane for which
the needle is vertical. Now tliis plane must be removed 90° from
the magnetic meridian, for in such a plane tho horizontal magnetic
force oi the e^th would have no resolved povtiou acting in the
plane of the needle's motion, so that the needle would practically
bo under the sole influence of the vertical magnetic force, and would
therufore point in a vertical direction. By this means therefore w«
obtaiu the magnetic meridian, and thus know the jilane in which
we ought to swing the needle. Tho needle must now be read
in the following positions :— (o) face of instrument east— (ace of
needle to face of instrument ; (/3) face of instrument west— face of
needle to face of instrument ; {y) face of instrument west— back of
needle to face of instrument ; (5) face of instrument east— back of
needle to face of instrument Finally, the poles of the nceiUe must
bo reversed, by rubbing them ivith powerful bar magnets in a
direction opposite to that in which they were previously rubbed,
and four observations taken corresponding to the above. The mean
of the eight observations so obtained will give us the true dip.
The turning round of tho face of tho instrument from cast to west
is made to counteract any error due to erroneous setting of the
vertical circle. The reversal of tho face of tho needle is made to
counteract any error due to the centre of gravity of the needle not
being quite coincident in the diiection of the needle's breadth with
its axis of motion, and likewise any erior due to want of symmetry
of the magnetic axis. The correction foi excentiicity is made by
reading both ends of tho needle. Finally, the reversing of the poles
of the needle is intended to counteract any error due to the centre
of gi'avity of the needle not being coincident in tho direction of the
needle's length with its axis of motion.
Dr Jouie^ has suggested a modification of the dip ciixle in which
the needle is hung on fine threads on which it rolls instead of rest-
ing on agate suppoi-ts.
5. Horizontal Force Magnetometer. — The theory of tho instrument
for determining the horizontal component of the earth's magnetic
force has already been given in the article Magnetism, vol. xv.
pp. 238 4^., and the instrument is shown in two forms, ibid.,
hgs. 28 and 29. The corr=ctions necessary for accurate results are
explained in a paper by G. M. Whipple (Froc. Roy. Soc., 1877).
(fl) Imtrumenls adapted for Travellers by Land.
6. Declinometer. — For travellere by land the unifilar instiument
(§ 2), mounted on a trip/d stand and duly levelled, is perhaps the
most accurate kind of declinometer.
For this purpose it is furnished with a transit niftror by means
of which an image of the sun may be thrown into the field of view
of the telescope, and — the geographical position of the station as
well as tho apparent time of the observation being known — an
azimuth thus aetermiued. In order that such an observation may
succeed, the following points must receive attention.
In the first jilaco the axis of the mirrer must be horizontal ; the
adjustment for this is made by means of a riding level. Secondly,
the normal to the plane of the iniri-or must bo perjiendieular to the
axis. Tho adjustment for this is made by a screw attached to the
back of the mirror. Take some object sufficiently elevated and
reflect it into tho telescope, getting tho object bisected by the wire
of the telescope. Then reverse the minor in its bearings. If tho
object remains still bisected by the wiro no correction requires to
bo made, but if not the screw at the back of the mirror must bo
moved until tho object is in precisely the same position in both
observations. Thirdly, the line of colUmation of the telescope must
be perpendicular to the plane of the mirror. In order to obtain
this there is a colhmating eye-piece a_ttached to the telescope by
which the sun's light may be made to" illuminate the cross wires.
Now turn the transit min'or until the reflexion of tho illuminated
cross wires coincides with the wii-es themselves, in which case the
line of collimation of the telescope must be perpendicular to tho
plane of the mirror. "When this correction has been once made, noty
the circle reading of a small vernier which moves with the mirror
and always set the mirror so as to give this reading.
' Ptoc. Lit. and Phil. Society, Manchester, voL viii. p. 171.
160
METEOROLOGY
[lEErvESTMAL JUGJTETISM.
By these means an accuiate reading of tho sun's bearing may be
made ; and, the position of the place and tho time of observation
being known, there are tables which enable the azimuth to be at
unce detenniucd.
7. Lloyd's Method of Dclermining ihe Total Fores.— While the
dip circle and the horizontal force magnetometer may be used by
travellers iu addition to tbeif use as observatory instruments, the
Rev. Dr Lloyd has devised a new method of determining the total
fcrce. Tne ordinary method of obtaining this is first to find the
dip and the horizontal force, from which the total force can be at
once deternJ' led by tho equation,— total force »= horizontal force x
secant din. This method is, however, open to objection in high
magnetic la!, tudes where the horizontal force is very smill and the
Jip approaches 00°. Now in Lloyd's method tiis objection is over-
tome. ^ Another circumstance which renders his method peculiarly
convenient for high magnetic latitudes, whore a traveller's equip,
ment must be kept as light as possible, i.'; the fact that it only
requires the addition o£ two needles to an ordinary dip circle in
order to give the required determination. These needles must be
carefully kept from contact with other magnets, and their poles
never revcr.
Here as before we have two unlcnown qn.antities to determine, the
one being the magnetic moment of the reagnet and the other the
total force of tho earth. We must, therefore, obtain two results,
the one embodying the product of the earth's total force into the
magnetic moment of the needle, while the other gives the ratio
between these two quontities.
8. In order to determine the former of these, let the needle
have a grooved wheel of radius r attached to its axle as in fig.
21, and over this wheel let an accurately knosvn weight W be
r
Via. 21.— Dip Circle,
suspended by means of a very fine silk thread. The best way of
doing this is to have a thread with two hool^s of precisely equal
weight at each end and then attach tho preponderating weight W
to one of these hooks. When this is done a new position of equili-
brium will be taken by tho needlo. If wo suppose that ?« denotes
,the magnetic moment of the needlo, that i is the angle of dip at the
place, and that »| denotes tho angle which the needlo in its deflected
position makes with the horizon, tho weighting being so made
that 5) shall bo less than i, then it is clear that tho needle h*; been
deflected out of its position of equilibrium through an angle i-n.
If we call this angle u and ticsignato by K the total force
»t the place, wo obtain the following equation of equilibrium : —
mRsinM = Wr (1),
on the supposition (which is very nearly hut not strictly correct)
that W denotes a constant force at all latitudes.
9. Next, in order to determine the ratio between this needle's
force and that of the earth, let it bo removed and employed to
ilcloet another substituted in its pis
When using it thus p.p a deflector -'t should bo laid iu a fiamc in
an invariable position as in fig. 21. This fran:e is at right angles to
tho line between the two microscopes, and as both pieces movo
together the best plan is to turn the v/holo round until the deflected
needle k visible in the centre of the field of the microscopes, in which
position it is of course perpendicular to the deflecting needle. By
always keeping to this arrangement we secure an invariable distance
between the poles of the t^vo needles. Suppose therefore that we
have employed the needle as a deflector in the above manner, ami
that the deflected needle has thus been made to assume a position
denoting an angle ij' with the horizon. It has therefore been
deflected from its position of equilibrium by an angle i - ij' (i denot-
ing the dip as before); calling this angle of dcHcxion u\ we obtain
the following equatijU of equilibrium : —
Ksiuu' = ?nTJ (2),
U being a function depending upon the distance of the needles and
on the distribution of free magnetism in them.
10. If we multiply together equations (1) and (2), we obtain
K-sinMsinw' — UWr (G),
in_ which w, u' are determined by observation, while W and r may
be regarded as constants. U is, as we have said, a function de-
pending upon the distance of the two needles and upon the distri-
bution of free magnetism in them.
The magnetic moment of these nedles is of coarse liable to altera-
tion, but if they are carefully guarded from contact with magnets
we may imagine that while their intensity alters, becoming weaker
for instance, this nevertheless does not .scnsiblj^ aflcct the distribu-
tion of the free magnetism within them, in which case the function
U may be regarded as a constant quantity. The results obtained
by this method of Lloyd's fully confirm this hypothesis regarding
U ; but it is essential that tho two additional needles, the deflector
and the deflected needle, should have their poles at no time either
reversed or disturbed.
Assuming therefore the constancy of tho quantity tT, its vaine may
be easily determined at any base station where the total force has
been determined independently by the ordinary method.
11. Having thus determined the value of U, or at once of tJWr
(which we may call c), let us carry our instrument to a diflereut
staliou and make the- requisite observations. We thus obtain
As this mettled is specially adapted for high lati^ades, the dip circle
employed (fig. 21) ought to be one for which the agate supports are
horizontal, so as to admit of the needle being visible when the dip
is nearly equal to 90°. It will also be noticed that, if the deflecting
needle have the same temperature when it is used in equation (I)
which it has wheu used in equation (2), then m iu the one case ie
strictly equal to m in the other, and thus no temperature con-ection
is rendered Eecessary.
12. A slight modification of the method now aeseribed is some-
times adopted. Instead of employing separate weights, which may
be easily lost, two small holes are bored in the deflecting needle
near each end. The one of these is filled with a suitably heayy
brass peg when the observations are to be made in the higher
magnetic latitudes of the northern hemisphere, and the other is
filled in a similar manner when the observations are to be made
near the' southern pole. In thU case therefore we must readjust
the instrument as we pass from the one hemisphere to the other, '^^i
slight change must be made in the fonnula when this method is
adopted, for it is clear that the weight will not now act always at
the same constant leverage. If the weight be called W and its
leverage when the needle is horizontal r, we shall have to modify
equation (1) as follows-
))iKsin«='Wrcos7i (B).
Equation (2) will, however, remain unaltered, and hcnco equation
(3) will become
n'siniismu'-UWrcoa (6).
If tho quantity XTWr bo determined at tho base station and called
c', wo shall havo
■/.
siuusinu'
(^:
(7) Instrumtnta adapted for Travclkra oy Sea.
13. Azimuth Compass. — At sea tho declination is generau/i
observed by means of an azimuth comiiasa invented by Kater.!
This is exhibited in fig. 22. It consists of a magnet with B
graduated compass card attached to it At tho sido of tho iustm-'
ment opposite the eye there is a frame which projects upwardsl
from tho plane of the instrument in a nearly vertical direction, and
this frame contains a wide rectangular slit cut into two parts by
a wire extending lengthwise. Tho eyopicco is opposite this framo,
and tho observer is supposed to point the in3trume"t in such •«
FiQ. 22. — Azimuth Compass.
rEKBESTKIAI. HAGNETJSM.
manner that thowire above nicTi'toueJ shall bisect the sun's nsiblo
disk. There is a totally leflcctiiit; gl4iss pri&m which throws into
the e3'e-piecc an imago of the scale of the graduated card, so that
the observer, having first bisected the sun's disk ty the wire,
must next read the division of the scale which is in the middle of
the field of view. Ho thus obtains a reading of the sun's position :
let us call this 100*. From this,
knowing the geographical posi-
tion of his station and the time
of tlie observation, he may de-
duce an azimuth ; let us imagine
that this is 70' W. Thus a
reading of 100" corresj^nds to
a position 70° W, Suppose next
that the instrument is so ad-
justed that when the magnetic
axis of the magnet is between
the eye-piece and the wire the
reading is 0". It is thus clear
that the magnetic meridian is
1.00° removed from the position
70" W. Let us imagine that the instrument is so graduated that
this denotes a position 30° E. We have thus obtained the mag-
netic declination. If the vessel be at rest the plan generally
adopted is to take the reading of the sun when rising and also
when setting; a mean between the two will give that which cor-
responds to a geographical meridian.
. 14. Fox's Dip Circle.— This instrument, contrived by Robert
Wero Fox, is more especially useful for observations at sea. In
this case it must be placed on a giraball stand and duly levelled
before commencing the observation. The following are the peculi-
arities of this instrument : — (1) the needles have two fine pivots or
axles which are inserted into jewelled
tockets ; (2) in order to avoid parallax
there are two graduated circles, the
one farther from the eye than the
other, and when reading the needle
the eye is to be so placed that pre-
cisely the same reading shall be given
by botii circles, — the true position of
the needle being thus obtained ; (3)
there is a rubber made of bone or ivory
«nd roughened, the object of which is
to rub a prolongation of the socket on
the back of the instrument, — the fric-
tion which this rubbing causes enabling
the needle to find its true position;
(4) to avoid as much as possible all
effects due to frict;on and adhesion,
the entire socket arrangement may be
turned round. TheaxK'S of the needle
•re thus compelled to be in contact
with a different set of particles. An-
other way of varying the suspension
is to use a magnetic deflecting arrange-
ment attached to the back of the
apparatus. Suppose that a reading
of the position of the needle so de-
flected is now taken. Next reverse
the position of the deflecting arrangement, which is done by turn-
ing a movable circle attached to this arrangement 180" round; let
the position of the needle be again read. On the hypothesis that
the needle is equally deflected on opposite sides of its true position
in these two observations, the mean reading will give the true
dip. ^ The principle of the method of observing with this circle is
precisely the same as that already described for observations on
shore with an ordinary inclinometer.
15. Fox's Intensity Arrangement is merely a modification of that
introduced by Lloyd, and already described in § 7.*
(8) Differential Magnetometers and Self- Recording
Magiutographs.
16. In addition to determinations at fixed intervals of time; it is
• point of much interest and importance to keep a continuous record
©rail the magnetic changes which take place at a few selected
•tations. This is accomplished by means of difTerential magneto-
meters. It is, however, necessary to continue to use absolute
instruracnta side by side with differential magnetometers, because
the latter (with the exception of the declination instrument) are
badly fitted for recording changes of long period, such as the secular
changes of the horizontal and tbe vertical force. The reason of this
will presently be seen.
' A great deal of detafled InforroaHon regarding Instmmenta for absolute deter-
mination and the merhouR t ' obscnrlng with them Is to be fonnd In the Admiralty
Uanuat 0/ Scientific Inquiry in an article on "Terrestrial Maffnetiani," by Sabine
xM E T E O R O L O Q y
161
17. Early in tho history of such instruments It was found tnat
hourly observations were exceedingly laborious, and attempts were
made to construct a set of self-recording magnetometers. The first
set of such instruments which were brought iuto systematic opera-
tion were those devised and constructed by the late Charles Brooke,
which have been at continuous work in the Greenwich Observatory
since 1848. In 1857 John Welsh devised a fresh set of self-record-
ing instruments, and introduced them into the Kew Observatory.
These, with certain slight modifications, have formed the type of
instruments supplied to a large number of magnetic observatories
all over the globe.
18. As we cannot conveniently record changes of dip by a
drflerential instrument, changes of vertical force are measured
instead by a balance or vertical force magnetometer. We have thus
in a differential system, whether adapted to eye observation or to
continuous photographic registration, three instruments, uaraely.i
the declination, the horizontal force, and the vertical force mag-
netometers or magnetographs as the case may be. Tho most
recently constructed instruments are adapted both for photographic
registration and for ej'e observation through a telescope. Tho
advantage of eye obser\'ations is that wo see what is taking placft
at the very moment of its occurrence, whereas we only obtain the
photographic record son^e time after the changes to which it relate^
nave actually happened.
Wo shall therefore describe — (a) the three instruments of the Kew
pattern as adapted to eye observations ; (fi) these instruments ai
adapted to continuous registration by photogiuphy ; (7) the method
of determining their scale coefficients ; (8) the method of determin-,
ing the temperature coefficients of the force instruments.
19. Kew Instruments — Eye Observations. — Fig. 23 shows us these
instruments arranged in the relative positions recommended by
Lloyd so as magnetically I'o interfere with one another as little as
Fio. 23.— Kew Instruments.
possible. We are supposed to be viewing the whole from tho sontb.
No. 1 to the right is the declination instrument. No. 2 that for
the horizontal force, and No. 3 in the distance behind the central
pillar (No. i) the vertical force magnetometer. Figs. 24, 25, 28
give us the details of these three instruments in the same order as
above. Connected with each instrument there is a circular mirror,
or rather two semicircular mirrors, made of perfectly plane glass.
One semicircular half of each mirror is attached to the magnet
and moves with it, while the other half is firmly attached to the
marble slab. Each magnet is enclosed in a gun-metal cas9 with
windows of perfectly plane glass ; each gun-metal case is covered
with a glass shade ; and the whole is air-tight, and capable ol
exhaustion. Each magnet too is provided with a copper damjiei
with tho view of checking its oscillations. In fig. 23 v/ill be seen
two pillars of smaller size. The right-hand pillar carries a tele-
scope, with a scale attached, to record the position of the declination
magnet. The scale is reflected from the semicircular minor moving
with the magnet, and the position of this reflected scale as viewed
in the telescope indicates the position of tho magnet Tho optical
arrangement for the other instruments is similar, except that the
vertical force mirror has a horizontal and not a vertical aiis.
The telescopes for viewing the force instruments are attached to
the left-hand pillar of smaller size.
20. The Dtdinmneter * (fig. 24) consists ot a magnet about 5 inches
long suspended by a silk thread freed from torsion as completely aa
For a detailed account ol tbB SjgV nUflSCtognph^
XVL — 2X
m
METEOROLO G>T
j>ossiblc. To Iccep the stato of the thread constant the class snade
should be rendered air-tight, and should contain some substance for
absorbing moisture, such as chloride of calcium. It is clear that
■J" tho state of the thread remains
tho same, and if tlie position of
the magnetic axis of the- magnet
does not change, this iustiimient
should record faithfully the various
changes of declination.
Tho Horizontal Force Mag7teto-
Tncitfr is exhibited in fig. 25. Here
the magnet* has been twisted round
into a position at right augles to
the magnetic meridian. It is sus-
pended by means of two very fine
«r,eol wires some little distance
apart, and thus the instrument is
olten called the bifilar magneto-
meter. These wires have tho piano
passing through their lower ex-
tremities differing very consider-
ably from that of their upper. If
the magnet a'lould suddenly lose
its magnetism the whole arrange-
ment would bo twisted round until
the two planes coincided. This
difference of plane gives rise to a
couple tending to twist the magnet
round in one direction while tli^^
horizontal magnetic force of tt,
ff'Tth constitutes an
■ecjUal and opposite -^t=—
coaple, the two couples "-
keeping the magnet ii
equilibriuuL Thecouj*!-'
depending upon the bi- __
filar arrangement may -^^^^
for the present be re- ^~"^*^^
garded as constant, that . , , ,
depending on the hori-
zontal force of the earth as variable. If the latter increase or
diminish, the magnet will i;e slightly twisted round in one direction
or the other.
In tho Vertical Force Magnetometer (fig. 26), the magnet is
balanced by means of a knife-edge
resting on an agate plane. By
means of two screws working hori-
zontally and vertically the centre
of gra^'ity may be thrown to either
side of the point of suspension,
or it may be raised or lowered and,
the sensibility of the magnet when
balanced thereby increased or
diminished. These screws are so
arranged that there is a preponder-
ance of weight towards the south
aide of tho magnet. This is
neutralized partly by the magnetic
force tending to pull tho north end
do^vn and partly by a slip of brass
standing out horizontally towards
the north side. Let us suppose
the system to be in equilibrium at
a certain temperature ; if the tem-
perature rise (since brass expands
more than steel), the leverage of
the weight at the north side will
increase more than that of the
weight at the south. There vdW
thus bo a slight preponderance
towards tho north, and
this may be an-angcd
.so as to n:utralizo to a y - ~:-V-- -^^ '
great extent the de- > ' .- /^jjjl?'
iCreaso in tho magnetic ^^ .7'
jmoment which an in- r ^■\
crease of temperature ^^
produces. _,
21. Magmtograplis. Fio. 25.— Horizontal Force Magnetometer.
I — Tlio arrangement by means of which these instruments are con-
rvortod into self-recordingmagnotographs is very simple. In fig. 23
■wo see a gas flame burning behind a vertical slit and placed ond-
;Wise in order to render its light more intense. Tho light from
this illuminated slit passes through a lens, and being reflected
from the mirror of the declination magnet throws an image of tho
I TBRni^sTKiAii maoneti&h:|
slit upon some sensitized paper in the central box. To spealc|
more properly, two images are thrown, one rcllocted from thcupperf
and movable half and the other from the fixed half of tho mirror.T
The sensitive paper is wrapped round a hori/onlal cylinder (fig. 27)A
and the tvvo unagas are tnercfore thrown upon diflcrcnt vzvXs^ ojft
> All tbo msgaeta are of tbc eaiDc sUa
this cylinder. But before reaching the cylinder these trvr imagei^
are by means of a hemicyLLndiical lens (shown in fig. 27) crushed
up into two dots of light. The cylinder moves round regularly by
clock-work once in twenty-four houi-s, and hence the eourse on th?
moving paper of the dot of light which comes from the fixca Iwa*
mirror will be a straight line, wliile that of the dot from the
moving half-mirror wUl be a curved line dependijjg on the motions*
of the magnet. When the paper is developed these lines appear
black.
The arrangement for the horizontal force instrument is precisely J
similar to that for the declinometer ; for the vertical force it ie
somewhat different, the illumuiated slit being horizontal and not
vertical, while the mirror oscillates on a horizontal axis and not on.
■ vertical one ; the hemicylindricai lens too and the cylinder are
•■ rtical and not horizontal. It was found necessary to put the
1 lane of motion of the vertical force magnet 15° out of the magnetic
iiieridian for the following reason. The axes of the telescopes are
respectively 30" inclined to the tubes which go fi-om t^" magneto-.
Fio. 27. — Magnetograph.
meters to the central box, and hence had tho vertical force magnet
swung in the magnetic meridian it would have been necessarj* to
place tho mirror inclined at the angle of 15" to the axis of motion
of the magnet. This was tried, but it was found that ib this posi-
tion of tho mirror the correction for temperature was so excessive
that the instrument became a thermometer and not a magnetometer. »
The mirror was therefore put in a plane passing through the axis'
of motion of the needle, the needle being made to move in a planet
inclined 15° to tho magnetic meridian.
22. Scale Cocjficicnts of Dijfcrcntiallnstrumcnis. — It is nocessaiyj
to know the value of one division of tho scale in the magnetometer,
or of one inch difference in tho ordinate of the curve impressed on'
the photographic paper in tho magnetograph. In the aeclinatioD
instrument it is only necessary to obtain the angular deviation cor-
responding to one division, and this may ho done at once by a seriod
of measurements. In tho horizontal andverliral force instruments
wo ^vi8h to obtain the value of one dinsion in pai t-s of force. There
is more than one method by which this can De accomplished, but
that of John Allan Broun is probably the simplest, and it is, w*
believe, the one adopted at most of tho various obsorvatories pos-
sessing self-recording instruments. It is given in the Bntiak
Association Reports^ 1869.
28 fevtpcraiUTe Coefficients of Dijjcrcntxai Force Instnivutax—n
Broiin has devoted a great deal of attention to tho subject of
these coeflTicicnts, and has come io tlic conclusjon that the beat
and most unobjecUonablc moLhoJ of determining them ib H5
iTBREESTKIAL MAGXETISM.]
MET E O R O L O a Y
1G3
compare tna instrumental readings on days when the tempera-
ture is high with the readings on days when the temperature is
low.
' 24. By differential instruments the components of a force affect-
ing the magnet are determined in three directions at right angles
lo each other. It does not, however, follow that this force is
entirely due to changes in the magnetism of the earth. We know
that certain forces connected with the sun affect the earth's mag-
netism, and on certain occasions at least these forces manifest them-
selves as currents in the upper regions of the atmosphere and in
the crust of the earth. Now such currents will have a direct effect
upon the needle as well as an indirect effect through the changes
which they may produce in tlie magnetism of the earth. The total
influence on the needle will therefore be made up of these two ele-
ments, the one denoting the direct influence on the needle of the
disturbing force, and the other the indirect influence through the
change produced in the earth's magnetism. No attempt has yet
heen made to separate the action of these two elements.
25. Self-recording instruments after the Kew pattern have been
supplied to observatories at the following places : —
Batavia.
Coimbra (Portugal).
Lisbon.
St Petersburg. '
Florence.
Stonyhurst.
Utrecht (declination only).
Melbourne.
Mauritius.
Kolaba (Bombay).
Vienna.
Zi Ka Wei (China).
San Fernando (Spain).
Potsdam.
Nice.
There are also self-recording magnetographs of other patterns at
Toronto, Montsouris (Paris), Greenwich, Wilhelmshaven ?') Cape
Horn, and Havana (!). ^
We understand that Professor W. G. Adams is at present
engaged in making a comparison of simultaneous curves from vari-
oos stations of these lists.'
. Magnetic Poles of the Earth— Secular Vaeiation.
28. Magnetic Foks of tU Earth.— In the article Magnetism it
has been shown that Dr Gilbert of Colchester had at a very early
period grasiped the important trath that the earth is a magnet, a
tmth which was afterwards mathematically demonstrated by Gauss.
It was reserved for Halley, the contemporary of Newton, to show
that the earth must be regarded as having two poles in the northern
and_ two poles also in the southern hemisphere, so that, unlike
ordinary magnets, its magnetic system has four poles altogether.
Before proceeding further it will be desirable to state what it was
that Halley acturfly did and what are the conclusions to be derived
■from his investigations. It has been remarked by Professor Stokes
that, while in an ordinary bar magnet wo may practically re<^rd
the pole as having a pliysical reality and as being the cause of well-
known attractions and repulsions, we are not entitled a priori to
assume that a point of maximum force in a large spherical magnet
like the earth must necessarily be the seat of attractions and repul-
sions after the same manner as the pole of an ordinary bar magnet.
It is to be determined by observation to what extent the earth
actually preserves an analogy to an ordinary magnet. Now Halley's
conclusions were derived from the pointing of the declination
needle, since in his day there were no observations possible on total
magnetic force. Ho argued that there are two points or poles in
the northern hemisphere to which the needle appears to be attracted,
one in the upper region of America and one above Siberia. So far
this conclusion is hardly anything more than a formal one derived
.from the grouping together of observations. He asserted that these
would be as they are known to be if we imagine two such poles or
foci of force each exercising a causal influence on the magnetic
needlp. And the justification of Halley's way of regarding the earth
is found in the fact that when force observations came to be made
two such foci of force were actually found to exist. We do not,
however, mean to imply that these foci have causal properties
exactly similar to the poles of a bar magnet, for this is not the
case.
In order to exhibit the process of reasoning which led Halley to
his conclusion, let us first imagine that the earth has only a single
pole or force-focus in the northern hemisphere, and that this is
coincident with its geographical pole ; then, assuming that this
pole has a causative influence on the needle's declination, we should
'•.meet all needles to point everywhere due north. It, however, this
pole be not coincident with the north pole of the earth, let us draw
a meridian circle passing through the magnetic pole and complete
It round the earth so as to divide the earth into two halves. At all
points in this ineridian circle the needle might be expected to point
due north while in the one half of the earth so divided it should
noint to the east and in the otlier half to the west of true north.
In the next place let us imagine that the earth has two north mag-
netic poles or foci of equal strength, both being at the same latitudl
while their difference in longitude is 130°, and let us draw a com'
plete circle of meridian passing through these poles (fig. 28V Let
us start from a point in this circle
under one of these poles and pursue
our journey eastwards along a circle
of latitude. At first the needle will
point due north. As we move east-
wards the needle will point west-
wards to the pole we are leaving
until we come to a region half-way
between the two poles, where it will
be equally solicited by each, and
will tnerefore .again point due north.
Let us call the space we have travel-
led over since we set out A. As we
proceed the needle will now be under
the predominant influence of the
second pole to our right, and will therefore point to the east
until we arrive at the meridian under the second pole. This second
space which we have travelled over let us call B. As we proceed
we pass through a space C where the needle again points to the west
until being once more equally influenced by the two pedes it will
point due north. After this we pass through a space D of easterlv
variation until we arrive once more at the point from which wo
started.
'Weo
3 Ills putllshera Messrs Sampson Low £
r- >, i '"^''"•'J"" 10 Mr Gordon_«nd r--.— . -.=«... ^.,v^.. ^..w o.
1,0., who have obUlned them (or us— for the sketches of the Instniments for
otjsolnte determinaUons, with the exception of that of Kater's compass, for which
w»«ro Indsbtcd to Mr J. J. BIcks. For the sketch of the aelt-recordhig mai;-
9 indebted to the Kew committee and to
Thus there are now four spaces instead of two, and these ar.>
shown in fig. 28, where the centi-e of the circle represents the north
geographical pole of the earth, and its circumference the equator
If pole 2 ba inferior in power to polo 1 the spaces B and C will be
smaller in size than A and D.
27. This last is an arrangement of things that agrees very well
with the results of observation, if wo add that the two poles are not
precisely 180° removed from one another in longitude. Fig. 30 4
represents lines of equal magnetic variation in 1882. There are two
lines extending throughout both hemispheres at all points of which
there is no variation, and also an oval-shaped district in the
northern hemisphere throughout all jioints in the circumference of
which we have no variation. These facts are inconsistent with the
hypothesis of a single pole, but they are quite consistent with that
of two poles or foci of force, one in northern America and the other
in northern Asia, the former being stronger than the latter. In
order to see this let us take our stand at the great line of no varia-
tion which passes through North America and travel eastwards.
We are just south of the American pole or focus, while the Asiatic
pole or focus is nearly 180° off, and hence the needle points due
north. As we proceed eastwards we leave the American or strongest
pole to the westward of us, and hence we have a region of west
variation which we have agreed to call A. As we begin°to approach
the eastern side of Europe we get nearer the Asiatic pole or focus,
and at length the line of no variation is reached, the tendency of
the American pole to pull the needle to the west being balanced by
the tendency of the Asiatic pole to ])ull it to the east. After this",
easterly variation predominates throughout a region B until at
length we come to a point in the western boundary of the oval where
we may imagine ourselves to be directly south of the Asiatic pole
while the American pole is nearly 180° distant; once more the
needle points due north. As we still travel eastwards wo leave the
Asiatic pole, which is now the predominant one, to our left) and
hence we have here a region C of westerly declination. At length
we come to the eastern boundary of the oval, where the tendency of
the Asiatic pole to pull the needle to the west is balanced by the
tendency of the American or stronger pole (acting now towards the
right) to pull it to the east, so that we have once more a point of
no variation. After this the American pole predominates, and we
have a large region D of easteriy variation until we travel round
once more to the point from which we started.
28. This train of argument receives, as we have already men-
tioned, corroboration from the fact that in the map of total force we
perceive two foci of maximum force, one in northern America and
the other in northern Asia, that in America being the strongest.
This evidence was not, however, in existence at the time of Halley,
and his hypothesis of two poles does the greater credit to his
sagacity, inasmuch as he had to deduce it from a comparatively
small number of observations of declination and dip, those of force
being altogether wanting.
29. We have hitherto spoken of two poles or, more properlv,
foci of maximum fora:, the positions of which are of course best
pointed out in fig. 29 ; but we have seen that the existence of such
^ Wo arc Indebted .for the admirable charts given in figa. 29-32 to the kindness
of the hydrographer, Captain Sir Frederick Evans, who, In order to save time
BUowed us to make use of the information he bad embodied even before it w«»
ofBclaU? published, and who likewise placed his plates at onr disposal
164:
METEOROLOGY
[ti:belsxbiai. maqkxhsil.
foci was first conjectoied from the bohaviour of the lines of
variation or declination. Now it mil bo noticed by looking at the
rariation map (fig. 30) that all the lines of equal magnetic variation
appear to converge to a point in the extreme north of the American
continent. This point is not, however, coincident with the chief
focus of force, which lies decidedly to its south ; but it is no doubt
coincident with the point denoting a dip of 90°, the locality of
which may bo inferred from the map of m:;gcctic dip (fig. 31), aul
it is likewise no doubt coincident with the r.ositiou of a zero of
horizontal force which ir.iy bo inferred from the map of horizonlat
force (lig. 32). 'ITius we liave a point to the extreme north ot
America which has the foHov.'i:i^ properties : — (1) the various LncA
of uoclination converge to it ; (2) tne needle points vertically down-
wards at it ; and (3) tho horizontal force vaniahes at it At thit
Flo. 29. — The Earth's Magnetism as shown by the Distribution of Lines of Equal Total Force, in Absolute Measui'e (British miles), with tho
Position of the Magjietic Poles and Equator, — approximately for 1875.
point therefore the horizontally balanced needle, having no hori-
zontal force acting upon it, will point in any direction.
I This point is, strictly speaking, the pole of vertirity, bnt, inas-
much as there is only one such point in each hemisphere, these may
for convenience sake be termed the magnetic poles, so that we speak
of two centres or foci of maximum force, and one pole in each hemi-
sphere
In the northern hemisphere Sir Frederick Evans* assumes tho
stronger or American focus to be in .52° N. and 90° W., and tho
weaker or Siberian focus in 70° N. and 115° E. In the southera
hemisphere he assumes the position of the stronger focus to be 65*
S. and 140° E., and of the weaker focus probably 6U° S. and 130° E.,
these being thus not far separated from each other or from tha
magnetic pole. The nearness together of the southern foci is prol^
East Vu^aQen
Wctt Vanaooa
rCAnVATUbaa
WaM VvuUS
jKiq. so.— Lmes of Equal Magnetic Variation, 1882.
'ably the reason why tho total force is greater at tho southern than
lit is at tho northern foci.
The magnetic pole (of vorticity) in the northern hemisphere was
Teached by Sir James Ross in 1831. The position of vertical dip
was observed by him to bo 70° 6' N. and 90° 43' W. Tho m.ignctio
pole (of verticity) in the gouthora hemispboro was nearly attained
by tho same navigator in a voyage made in 1839-M. Its positii»w
is probably 73 J° S. and nrj'li-
The lino of no -'ip is called the magnttic or dip equator — itt
position is given in tigs. 29 and 81. Tho lino connecting all thu
> eimcntan MamaXM lU Batatim tftUt (tavou te Ava Bklpi.
■XSESSTEIAL MAONXTliiU.]
METEOROLOGY
165
•points where the mijnctic intensity is least is called the dynamic
equator. It coincides very nearly with the dip equator.
80. Secular Variation. — The e^rth then as a maffnet must be
supposed to have two sets of centres of force. AN e shall next
attempt to show that these centres cannot be regarded as constant
faoth in position and intensity.
It should be cremised thati while there is no well-established
e'ndenco to show that either the pole of verticitj' or the cectro of
force to the north of America has perceiitibly changed its place,
there is, on the other hand, very strong evidence to show that wo
have a change of place on the jiart of the Siberian focas and also on
the part of its analogue in the Bouthern hemisphere.
Table 1. (p. 166), given by GUpin {Phil. Trr.na., 1806),> exhibits
the change in the position of the needle in Great Britain from
Fio. 31. — Lines of Equal Magnetis Dip, 1882.
the earliest obsenrations np to the beginning of the present
century. " " : ■ -
SI. Between the dates recorded in this table the needle has been
pointing more and more to the west, which implies either a relative
ucrease in the power of the American as compared to the Siberian
focus, or a motion of the Siberian focus from west to east On the
first supposition the lines to the eastward of the SibeHan focus —
for instance, the line ofno variation depending on a balance between
it and the American focus — should be drawn in towards it, or they
should travel westwards ; but if the latter supposition is true, or
this focus has been moving eastwards while retaining its force, the
lines to the east of it should be found moving eastwards also. There
is strong evidence that the latter is the case, and that in the
northern hemisphere there has been a long-continued progression
^IG. 32.— Lines of Equal Horizontal Force, 1882.
to the east^'ards of the system of magnetic lines on toth sides of
the Siberian focus. In the southern hemisphere also we have proof
that the analogous focus has been travelling, not from west to east,
but from east to west.
S2. There "s some reason to believe that the eastward motion of
thySiberian focus has been recently reversed, and that it is now
going from east to west. Table U. shows the declination observed
at Bushey Heath (Herts) during 1817-20, and at Kew from 1868
to 1882.
It would appear from Table II. that the maximum westerly
declination was reached in 1818, and that the needlo has since that
date been travelling eastwards. A similai- change has taken place
I Taken from Walker'i Uofnelimt.
166
METEOROLOGY
[TEItEESTItlAL MA0KETI3M.
&t other stations ; and, altliougli these changes are not strictly
simultaneous at the various stations, they have yet been sufficiently
general and near together in point of time to indicate that some
Table I.— Secular CItange of VaHaticm in Great Britain.
Observer.
Date.
Declination.
Mean AiinudI
Westward
Cliange.
1580
1622
1634
1657
1665
1672
1692
1723
1748
1773
1787
1795
1802
1805
11 15E.
6 OE.
4 6E.
0 OE.
1 22 W.
2 30 W.
6 OW.
14 17 W.
17 40 W.
21 9W.
23 19 W.
23 57 W.
24 6AV.
24 8W.
Gimter
7
9
10
10
9
10
16
3
8
9
4
1
0
6
6
2
7
5
0
1
4
3
7
2
7
Cellibranil
Bond
Halley
Hallcy
Graham
Gilpin
change hxs probably taken place in the movement of one set of the
magnetic foci of force.
33. Halley sought to explain the four-pole theory and to account
Table II. — Changes of Declination in England,— at Bushcij Beath
for 1817-20, and at Kcwfrom 1858.
Declination West.
Declination Wost.
1817
24 36 4
1869
20 26 24
1818
24 38 25
1870
20 18 52
1819
24 36 14
1871
20 10 31
1820
24 34 30
1872
20 0 31
1858
21 64 8
1873
19 57 44
1859
21 47 22
1674
19 51 58
1860
21 39 51
1875
19 41 14
1861
21 31 36
1876
19 31 53
1862
21 23 32
1877
19 22 22
1863
21 13 16
1878
19 13 50
1864
21 3 35
1879
19 6 10
1865
20 59 3
1880
18 57 59
1866
20 51 10
1881
18 50 30
1867
20 40 26
1882
18 44 47
1868
20 33 9
Table IW.—Exh
ibiling certain Years' Values of Declination a
Varioui
Places.
' Toronto
\
Makerstoun.
TrCTandrum.
Cap
of Good Hope.
Hobart Town. 1
Declination
Declination.
Declination.
Declination.
Declination.
1841
1 14-3 W.
1841
25 33-7 AV.
1854
0 25-896 E.
1605
0 30-0 E.
1843
9 53-32 E.
1842
1 19
1 W.
1842
25 28
4 AV.
1855
0 26
026 E.
1609
0 12
0 AV
1844
9 54-93 E.
1845
1 29
1 W.
1843
25 22
9 AV.
1856
0 26
400 E.
1622
2 0
0 AV
1845
9 56-47 E.
1846
1 30
8 W.
1844
25 17
1 AV.
1857
0 27
278 E.
1675
8 14
0 AV
1846
9 58-42 E.
1847
1 S3
2 W.
1845
25 11
3 AV.
1858
0 28
769 E.
1691
11 0
0 AV.
1847
9 59-28 E.
1848
1 35
4 W.
1846
25 6
0 AV.
1859
0 30
406 E.
1751
19 15
0 AV.
1848
9 60-61 E.
1849
1 36
9W.
1847
24 59
6 \V.
JS60
0 32
034 E.
1775
21 14
0 A\'.
1850
1 38
6 W.
1848
24 51
8 AV.
1861
0 34
318 E.
1788
24 4
0 AV.
1851
1 40
9 W.
1849
24 45
2 AV.
1862
0 36
654 E.
1792
24 31
0 AV.
1856
1 56
3 W.
1850
24 39
0 AV.
1863
0 39
123 E.
1818
26 31
0 AV.
1857
2 0
5 W.
1851
24 31
3 AV.
1864
0 41
603 E.
1836
28 30
OAV.
1858
2 4
5 W.
1852
24 25
2 AV.
1865
0 44
007 E.
1839
29 9
0 AV.
1859
2 7
4 W.
■ 1853
24 18
7AV.
1866
0 46
310 E
1841
29 6
2AV.
1860
2 10
6 W.
1854
24 11
8 AV.
1867
0 47
590 E.
1842
29 5
9 AV.
1861
2 14
4 AV.
1855
24 5
8 AV.
1868
0 48
687 E.
1843
29 6
OAV.
1862
2 15
7 AV.
1869
0 49-735 E.
1844
29 6
2 AV.
1863
2 19
1 AV.
1845
29 7
4 AV.
1864
2 21
9 AV.
1846
29 8
7 AV.
1865
2 24
8 AV.
1847
29 12
4AV.
1866
2 27
6 W.
1848
29 14-0 AV.
1867
2 29
8AV.
1849
29 16 2AV.
1868
2 33
2 AV.
1850
29 18-8 AV
1869
2 37
1 AV.
1870
2 41
9 AV.
1871
2 47-9 AV.
1
Table IV.-
-Exhibiting certain Years' Values of Dip
ind Horizontal Force at Various Places
The years in this Table are from.
April to April ; th-us 1845 means the yea
rfrom 1st April 1845 to 3lst March 1846.
London
or Kew.
Toronto.
Hobart Town.
Cape of Good Hope.
Dip.
Hor. Force.
Dip.
Hor. Force.
Dip.
Hor. Force.
Dip.
1857
68 24-87
1857
3-7899
1845
75 15-60
1845
3-5476
1842
70 42-2
1846
4-5054
1841
53 9-1
1858
63 22
56
1858
3-7950
1846
75 14
58
1846
3
5419
1843
70 38
2
1847
4-5001
1842
53 15-3
1859
68 21
41
1859
3-8007
1847
75 15
30
1847
3
5384
1844
70 33
3
1848
4-4991
1843
53 20-2
1860
68 19
29
1S60
3-8063
1848
75 18
3-:>
1848
3
5339
1845
70 32
0
1849
4-4997
1844
53 29-4
1861
68 17
42
1861
3-8121
1849
75 18
94
1849
3
5367
1846
70 33
0
1850
4-4998
1845
53 29-3
1862
68 14
89
1862
3-8165
1850
75 19
98
1850
3
5322
1847
70 34
5
181.3
68 11
71
1863
3-8216
1851
75 20
42
1851
3
5299
1848
70 35-7
1864
68 9
31
1864
3-8284
1852
75 20
52
1852
3-5154
1865
68 8
50
1865
3 8306
1866
68 5
44
1866
3-8391
1867
68 2
62
1667
3 8467
1668
68 2
13
1808
3-8493
1869
68 0
41
1869
3-8551
1870
67 57
98
1870
S-8585
1871
67 56
12
1871
3-8640
1872
67 53
60
1872
3-8712
1873
67 51
19
1873
3-8777
1874
67 49-64
1874
3-8828
fTHaRESIElAL MAGXETISM.]
MLTEOROLOGY
167
for the secular change by imagining a solid globe or terella,' con-
centric with the earth but rotating independently of the external
shell and having a slightly different period of rotation,— the shell
having two jiolcs and the terella t^vo others. Wliile continuing to
adrniro Halley's saRacity, we shall not now be disposed to allow such
a constitution of the interior of the earth, but will rather be led to
look to some external influence as the cause of the secular variation.
\Vliile we have strong evidence that the Siberian focus has changed
its position, we cannot assert that the American focus has been
absolutely stationary, or that neither focus has experienced any
, changes of force. On these points we must be content to be gnided
by observation alone.
34. It has been supposed by some magnetjcians that it is pos.sible
to compute with something like certainty the particulars of the
motions of the magnetic foci. Hanstecn more especially (1811-19)
computed both the gcogi-aphical positions and probable periods of
revolution of this dual system of loci of force round the terrestrial
pole. Sir Frederick Evans has discussed in connexion with the sub-
ject all the most recent observations,- and points out two objections
to any such theory as that of Hansteen, -nz., (1) that, while a mag-
netic turning point has been reached in certain regions, there are
large portions of the earth in which this change has not yet been
accomplished, and (2) that in certain districts of the earth very great
ohangciJ in force have taken place. "If we turn," he says, " to the
continent of South America and its adjacent seas, we shall find a
liminution of the intensity of the earth's force now going on in a
remarkable degree. An examination of the recent ohser\'ations
made by the ' Challenger ' officers at Valparaiso and Monte Video,
:ompared with those made by preceding observers, shows that
.vithin half a century the whole force has respectively diminished
one-sixth and one-seventh,— at the Falkland Islands one-ninth."
On the whole, while there is strong evidence that the Siberian focus
has until recently been travelling eastwards, and its analogue west-
wards, and evidence less conclusive that recently a turning point in
this motion has been reached, we are disposed to think with Sir
Frederick Evans that a formal theory like that of Hanstecn docs not
igree mth recent observations. We shall revert to this subject.
35. In Tables III. and 'IV. certain yearly values of declination,
, lip, and hoiizontal force arc given for various stations.
Inequalities in or connected with Terrestrial
Magnetism depending on the Sun.
36. As there is a marked likeness between th6"ways ia which the
3un dominates over the two great divisions of terrestrial phenomena,
meteorology and magnetism, let us endeavour to describe the
sun's effect upon tlie latter by referring to its influence on the
former, the chief peculiarities of which are well known to all. We
find that the temperature of the air at a given station is subject to
a diurnal fluctuation having its minimum value shortly before sun-
lise and its maximum early in the afternoon. We find likewise
that the mean temperature for the day, as well as the amplitude of
this diurnal oscillation, depends upon the season of the year, both
being greatest about midsummer and least about midwinter. Now,
if this were the only manifestation of solar influence upon this
particular element, it would be possible to pretlict the temperature
tor any hour of any day once the mean temperature, the diurnal
variation of temperature, and the modification of these for different
seasons of the year had been well ascertained. But this amount of
regulaiity is very far from takin" place, — the march of temperature
being frcq^uently interrupted, cloaked, perhaps even reversed, by
the advent of peculiar weather. Thus we may have very cold
"Weather in midsummer and very warm weather in midwinter, or
wc may have a very cold afternoon and a very warm early morning,
by which means tne ordinary conditions of temperature will be
completely reversed. In like manner weather interferes even to a
greater extent mth the diurnal oscillation of the atmospheric
pressure, so that, in British latitudes at least, it is only possible to
o'btain this correctly by means of a long scries of observations.
Weather, however, does not consist of a perfectly lawless inter-
ference with periodical phenomena, but is subject to laws of its own,
some of which we are beginning to discover. Sometimes weather
may exalt or depress the diurnal fluctuation of temperature without
otherwise affecting its character; but sometimes too the turning-
points and the general appearance of this fluctuation are greatly
influenced by peculiar weather.
' 37. Now it is believed that we have something of this kind in
those fluctuations depending on the sim to which the elements of
terrestrial magnetism are subject. Let ns take the declination
as the most easily studied of the three magnetic elements, and
suppose that we are engaged in considering the traces denoting the
fluctuations of declination as derived from a set of self-recording
magnetographs in Great Britain. Here we shall at once be able to
recognize in an unmistakable manner the diurnal variation depend-
ing upon the position of the sun, in virtue of which a freely-
» See Walker's Terrtttrial and Cosmical Magrutism^ where the snhject is well
^cussed.
'JtoUs lecture to the Royai Geographical Society, March II, 1878.
suspended magnetic needle reaches the easterly extreme of its range
about eight in the morning, and the westerly about two in the
aftenioon. We shall likewise perceive that the range of this
diurnal fluctuation is greatest at midsummer and least at mid-
winter. In fine, the characteristics of this fluctuation, depending
as they do upon the hour of the day and the season of the year,
are not very diflcieut from those exhibited in the diurnal fluctua-
tion of atmosphciie temperature. But, however thoroughly we
may have ascertained tlie mean declination and its diurnal oscilla-
tion, as well as the modifications of these depending on the season
of the year, we shall nevertheless find it impossible to predict the
exact position of a freely-suspended magnet at any moment of a
particular day. Hero then too we have something which may be
called magnetic weather, and which interferes with the regular
progress of the systematic fluctuations of the magnet. Magnetic
weather has, like its meteorological analogue, a set of laws of its
own, some of which wc are beginning to find out. Sometimes
magnetic weather may exalt or depress the diiumal fluctuation of
declination without affecting its character, but it is imagined that
at other times the turning points and general appearance of this
fluctuation may be greatly influenced by peculiar magnetic weather.
38. There is, however, a kind of magnetic change which, so far
as we know at present, is not analogous to anything in meteorology,
and introduces an additional element of complexity in any attempt
to analyse the fluctuations of terrestrial magnetism. We mean the
well-known magnetic disturbances or storms which occur simul-
taneously in places very widely apart. Under these circumstances
it becomes a question how we can best deal in a practical manner
with this complicated system of things.
Wo do not think that with our present knowledge any bettet
system can be adopted than that first inti-oduced by Su: Edward
Sabine in his discussion of the results of the colonial magnetic
observatories. Suppose that we have hourly magnetic observations
at a station, then firat of all we should arrange these into monthly
groups — each hour by itself. We should then reject as disturbed
observations all those which differ by more than a certain amomit
from their respective normals of the same month and-lianr, — chs
normals being the homly means in each month after the exclusion
of all the disturbed observations. This method enables us, by its
exclusion of disturbances, to ascertain mth much accuracy the true
form of the solar-diurnal variation of the magnetic elements at a
given place corresponding to every month of every year, providca
only that the observations are sufficiently numerous. On the other
hand it will probably fa0 in accurately giving us the variations from
day to day of the ranges of these dimnal fluctuations caused by the
advent of peculiar magnetic weather,— inasmuch as the records of
the extreme effects of such weather will probably be cut off from
the undisturbed observations and reckonccf among the disturbances.
For instance, it is known that the solar influence on terrestrial
magnetism varies from year to year, and it is suspected that there
are also short-period fluctuations of solar influence. It would not,
however, be a safe proceeding to attempt to estimate niunerically
this last-mentioned element of fluctuation by taking the successive
diurnal ranges of those obseiTations at any station, reckoned as
undisturbed, by the above process, and plottin| them as successive
ordinates of a curve, and then supposing that this curve would give
us a true graphical representation of solar changes. It would
rather probably represent such changes with the tops and bottoms
of the larger fluctuations cut off. But if the undisturbed observa-
tions fail in this respect we can hardly be wrong in supposing that
there has been eliminated from them, as far as possible, sol influence
due to magnetic storms, and hence that they will afford us a much
better means of estimating small'fluetuations, such, for instance, as
those due to the moon, than we could have had without their aid.
Finally, with regard to that portion of the observations selected
as disturbed, we are probably not certain that every such observa-
tion represents a true disturbance, or that the absolute times of
occurreuco of the various observations selected as distuibed at one
station will be the same as those at another. Nevertheless Sir
Edward Sabine has shown that at the Kew Observatory certain laws
of disturbance deduced from the whole body of observations selected
as disturbed are closely reproduced when this selection is made on
a narrower basis — ninety-five days of prominent disturbance being
alone taken. With these prefatory remarks we shall now proceed
to discuss the diurnal inequality of terrestrial magnetism.
39. Total Diurnal IncqualUy Defined.— It will be seen further
on that disturbed as well as undisturbed observations are subject to
a divuTial variation, but these two variations are different, and the
name diurnal inequality is generally given to the compound varia-
tion which is the joint resultant of the two. Solar-diurml
variation is that portion of the compound inequality which refers
to undisturbed observations, while that which refers to disturb-
ances has received the name of disturbance-diurnal mnatxon. It
would appear that in the United Kingdom, and perhaps through-
out Europe, the total diurnal inequaUty is not very greatly
different either in character or range from its most important
component the solar-diurnal variation, at least so far as^the.
168
METEOROLOGY
declination is conecrrei When the diumal oscillation of a freely-
sospenJcJ nia^ct was first observcil, tho subject of map^ctic
disturbances was not understood, and tho early individual deter-
minations which have been handed down to us are not such as to
justify t!ie cxiiendituro of any very great labour npon them for
the purpose of scjiarating tho disturbed from tho undisturbed obser-
Tations. Inasmuch, however, as tlie total diurnal inequality of
declination (which is in reality tho element given by these early
observations) docs not greatly differ from the solar-diurnal varia-
tion, we may with much justice and little risk of error give the
history of these early observations in connexion with that of the
solar-diurnal variation of declination, which is by far the best
known, and perhaps tho most important, of all the various magnetic
changes protluccd by solar inducnce.
40. Solar- Diurnal Vnriation of Declination. — Graham, an instru-
ment maker of London, discovered in 1722 that a freely-suspended
ma'Tictic needle is subject to a diurnal oscillation of definite char-
acter.' The next obscrvci vias Canton, who in 1756 bc^n a series
of nearly four thousand observations, which he communicated to the
Royal Society on December 13, 1759, and from which he concludts
that the range of the diurnal variation is greater in summer than in
wriuter. Macdon.ild's oteervations at Fort Marlborough in Sumatra
in 1795 [Phil. Tram., 1796), and Duperrey's in the tropics in 1S25,
were perhaps the first that might lead us to conclude that the
amplitude of the diumal oscillations of the ncedjc is less in the
tropics than in middle latitudes, and that the motion of the needle
in the southern hemisphere is in the opposite direction to that in
which it moves in the northern hemisphere at the same hour.
41. SemianmuU Inequality.- — The existence of these early
observations had led some magneticians prematurely to conjecture
that there must bo a line somewhere near the equator at which
there is no horary variation in declination. In 1347 Sabine com-
municated to the Roy::! Society the results of five years' observations
at St Helena, showing that at that station for the half of the year
beginning at the vernal and ending at the autumnal eqnir.oi the
motion of the needle corresponds nearly to that in the northern
hemisphere, whils: for the other half it corresponds nearly to that in
the southern hemisphere. Sabineafterwardsconfirmed and extended
his conclusions regarding the semiannual inequality by discussing the
results obtained at the various colonial magnetic ohser\'atoric^. More
recently, as the result of twelve years' observations at Trc-\andrum,
at an observatory established by the rajah of Travancore, Joiin
Allan Broun gave in a very complete form the laws of change
of the solar-diurnal variation of magnetic declination near the
equator, showing the extinction of the mean movement near the
equinox.
42. Perhaps the best way of exhibiting what really takes place is
the following, which is that adopted by Sabine.
The mean annual value of the solar-diurnal variation is of what
may be called the northerly tjTie in places of middle latitude in the
northern hcmis|>l:cre, and of what may be called the southerly type
in places of middle latitude in the southern hemisphere. Kow let
ns take a nonaem station, and consider the mean form of its solar-
diumal variation fcr tho six months beginning with the vernal
equinox. Here we shall have an oscillation of the northerly type
with a range greater than the annual range. For these six months,
therefore, we may imagine that the annual range has been s-apple-
mented by the superposition on it of a variation with a type similar
to its own. At the same station, during the other six months, the
eolar-diurnal variation is less than the mean of the year, as if the
annual variation had been depressed by the superposition on it of a
variation with a type the opposite of its own, that is to say, with a
southerly type. At a station in the southern hemisphere, again,
the mean annual form of tho solar-diurnal oscillation is of the
southerly type, reluced during the six months beginning mth the
venial equinox by the superposition on it of a variation of northerly
type, and increased during the other six months as if by the super-
position of a variation of southerly type. Thus when the sun is
north of the equator we may superpose a variation of the northerly
type upon both hemispheres, with the effect of increasing the ra^go
in the northern hemisphere and diminishing it in the southern ;
and while the sun is south of the equator we may superpose a varia-
tion of the southern ty[>e upon both hemisphcrcii, with the effect of
diminishing the range in the northern and increasing it in the
southern hemis[ihere.
Near the equator, an at Trevandmm, where Bronn made his
observations, we find the mean annual v.ilnc of the sokr-diurnal
variation to bo extremely small, if not altogether evanescent.
During the six months beginning with tho vernal equinox the typo
is entirely northerly, while for the remaining si:; months of the year
it is entirely southerly in character. In fine, at this station the
solar-diumal variation chances its character at the equinoxes, at
which time we have, as already observed, an extinction of the mean
movement, — not indeed an absence of all variation, but rather a
LTEKCrSTEIAL HAGKSTISM^
variation having .m nndccided character, which for a few days may
be of one tj-pe and then of tha very opposite. There is movement
but no moan movement. * -^
43. In the following table (V.) the solar-diumal variation is
given for Kew, Trevandrum, and Hobart Town. Of them-
places the first denotes a station in middle latitude (northern
hemisphere), the second an equatorial station, and tho third a
station in middle latitude (southern hemisphere).
•a
i|
Sew.
Trevandrum,
Hobart Town. 1
April
°,'^ Whole 1
April
Oct
Whole
April
Oct.
to
March.
Whole
<
Sept.
Slarch.
Vear.
Sept.
March.
Year.
Sept.
Year.
c
-CIS
-412
-5-13
-1-30 -fO-07 -0-CI
4-0-35
4-2 35
4-1-35
1
-7-42
-4«
-CIO
—1-25 -1-0-S5
-0-45
4-4-S5
4-3-50
2
-6-M
-4-C7
-5-Sl
-0-S5 -1-0-5G
-0-15
4-3-15
4-5-95
4-4-65
3
-5-21
-3-3->
-4-23
-0-35 -1-OCl
-1-0-13
4-3-30
4-5-60
4-4-40
4
-3-25
-1-05
-2-CO
-1-0-03 -1-0-53
+0-2S
4-2-40
4-4-30
4-3-35
S
-147
-l-O-S -1-26
-1-0-15 •fO-33
4-0-24
4-1-30
4-2-70
4-2-00
e
-n-02
-9-40
-0-39
-1-0-05 -1-0-22
-1-0-13
4-0-75
4-1-5S
4-1-15
7
4-0-22
-fO-21
-fO-22
-0-15 4-0-.'3
4-0^14
4-0-20
4 OfO
4-0-60
8
-fO-44
-fO-92
-HO-68
-0-30 -1-0-19 -0-05
-0-.-!0
4-0-30
4-0-00
9
-)-0-52
-n-45
-fO-09
-0-28 1 -1-0-13 1 -009
-0-65
-0-25
-0-55
10
-)-0-70
-n-77
-n-24
-0-20
-1-0-09
-0-oc
-1 10
-0-70
-090
11
-HO -90
-fl-84
-i-1-37
-007
-j-O-IO
4-Ofll
-1-15
-0 85
-100
I-'
■fllO
-fl-C7
4-1-43
-1-0-07
-1-011
4-009
-1-10
-0-EO
-0-05
13
+ 1-Q3
-1-134
•4-1-20
-HO-18
-fO-03
4-0-13
-0-75
-0-75
-0-75
14
-t-I-55
-fl-22
-H-3D
-i-0-27
-HO-02 ; -1-0-15
-0-40 1 -0-70
-0-55
15
-nor.
-rl-OO
-1-1-51
-1-0-29
-0-11 1 -1-009
-015 1 -005
-0-10
IB
-(-2-69
-i-ii;
•1-1-88
-1-0-31
-0-23
4-0-02
-0-02 1 -0-78
-040
17
-f3-C0
-n-43
-i-2-51
-t-0-4S
-0-45
-l-OOl
-010
-1-40
-0-7;
13
-f4 59
+1-54
-f3-07
-t-1-02
— 0C6
4-0-18
-0-23
-2-37
-ISO
10
4-5-31
-1-1-8^;
-1-3-58
-1-1-48
-0-81
4-0-32
-0-50
-3-80
-2-15
10
-h5-20
■f2-40
-4-3-50
-1-1-20
—0-73
4-0 2!
-125
-5-25
SI
-1-3-57
-H2-32
-1-2-05
•fO-47
-0-3?
4-0-OS
-2-10
-5-30
-3-70
22
■f0-3S
-fO-54
-1-0-40
-0-32
-0-13
-0-22
-2-20
-3-SO
-soO
23
-3-lS
-2-lS
-2-68
-0-93 1 -0-07
-0-50
-1-40
-0-80 1 -1-151
« See Walker, Terrestrial and Cotmical Afa^etism.
* ThU ii the namo used by Sabine, tat iu appropriateness toaj perhaps bo
qaettloaed.
In this table deflexions to^-^ards magnetic east are reckcned positive; deflexion*
towards mapieilc west negative. The etale is in minutes of arc
Also in fig. 33 we have a graphical representation of the solar-
diumal variation for the whole yeajr at these three stations, from
which it will be seen that the range at Trevandrum is extremely
small, and that the cun-e for Hobart Town is opposite in appearanca
to that at Kew.
y
\
■«.
O-O
\
^.^- —
— -
''•■
'
\;
/
' h\
Ir,.
^^
\
/
.io
THeVAUOHUM.
1
1
^^
0-0
'h'/„.
~ h\
»5-0
HOBARTOVlft
-j'o
r
^-
— ! — " " s
1
J
^
r^
J
1
Fig. 33.
Finally, in fii;. 31 Tve have a graphical representation of the semi-
annual inenua'.ity or difference from the whole year's mean of the tv>
half-yearly means of Table V., tho one half-year (that with thick
lines) commencing at tho vernal and the other at the autumnal
equinox. It will be seen from this figure that the semiannual
inequality -is of tho same character in both hemispheres, the likeness
extending even to its minor peculiarities. i
44. Channc from Monlh to J/oii(A. —Charles Cliarabers, director
of the Kola'ba Observatory, Bombay, remarks { Trans. Jtoy. Soc,\
December 10, ISCS) that "the rcgtilar pr g.-cssion from monU
to month in tho diumal variation is so distinctly shown m tje
Bombay observations as to lead, on a first inspection, to tho
supposition that the law of variation is identical throughout th»
year, the extent only (including a reversal of direction) varying fiom,
month to mouth. But in this respect a lUITcrent einosiuon of tli«
character of tho variation in dilferent months shows that the
first thought would be inaccurate." Ho Uicu proceeds to <hMxm,
TEBBESTBIAL MAOXETISM.]
METEOROLOGY
at length the montlilv values of the solarJiumal Tariation at
Bombay. Broun has likewise (Trevandrum observations) discussed
«t length the solar-diurnal variation at the Trevandrum Observa-
tory. It would hardly b« of service to reproduce here the results
of these discussions; but when such analyses become sufEcicutly
.j'-5 —
KEW
'^
C\^
F
0 ^^
"^
1 ^ ^
><-
^
TncvA
ton
-J
5^
fr, -<
vy^
'"
/.oe../;r;
!il
«J
^T^N,
, /
^
T'
,
\y
1
Fig. 34.
extensive theyvmay be expected to throw light upon the cause of
the solar-diurnal variation.
In the following table wo have mean monthly values of the declin-
ation range at the Kcw Observatory corresponding to forty-eight
points in the year — derived from sixteen years' observations: —
Table VI.— Containing Monthly Means («ni<-22'04) /or Forty-
tight Points in the Year of the Kcw SoIar-DiurTial Declination
Banges. Thus Janwxry (0) gives the monthly mean of which the
middle dale is the very commencement of the year, January (1)
thatjor one week after the commencement, and so on.
McanVohie.
Mean Value.
JfaiaTslQct
Jan. (0)
■012
MST
(0)
•J99
Sept. (0)
•;94
(1)
•323
(1
681
(I)
•i77
(2)
-340
(2
•573
(2
K4
(3)
•362
(3
■iS6
(3
•532
Feb. (0)
•3£5
(0
■SM
Oct. (0
•613
(I)
•401
0)
•COS
(1
•40« 1
(2)
•418
(2
•CIO
(2
■478
(3)
•438
<3
•604
(3)
•463 1
ICarch (0)
•467
Juljr
(0)
■601
Not. (0)
■445
(">
•508
fl)
•i07
(<)
-418 ;
(2)
•54S
m
■501
<2)
•339 1
(3)
•5ST
M)
•503
<3)
•360 ]
April (0)
CIS
Aug.
(0)
•504
Dec. (0)
•340 1
<1)
6.12
(1)
•COl
(1)
•322
(2)
639
(■-')
■611
(2)
•308 1
(3)
■620
<3)
•606
(3
•303 1
It will bo seen from this table that, while we have a ma.timum
about the summer and a minimum about the winter solstice, wo
have unmistakable indications of maxima at or about the equinoxes.
This does not take place at a tropical station such as Trevandrum.
45. Behaviour near the Magnetic Pole. — Figs. 33 and 34 exhibit
the most prominent features of the solar-diurnal variation of declina-
tion in the extra-tropical regions of the northern hemisphere. If
an observer stand over the centre of the needle and look towards
thf marked end, or that which points to the north, he \vill perceive a
ddlcxion towards his right hand which will reach its extreme about
8 A.M. and a deflexion towards his left hand which will reach its
extreme about 2 P.M. But are these deflexions to the right and
left liand of geographical or of magnctical north ? This question
has beeu answered by Sabine in his discussion of the results of hourly
observations of the magnetic declination at Port Kennedy {Phil.
Trans., 1303, p. 660). This station is 72° 0' 49" N. lat. and 94° 19'
W. long., and here the marked end of the needle, while it points
towards the magnetic pole, points in reality about 35° to the west of
south. Now the marked end of the needle when viewed at S a.m.
is seen at Port Kennedy to have moved to the geographical west
but to the magnetical east It would thus seem that tlf.oughout
the extra-tropical regions of the northern hemisphere the 8 A.M
deflexion of the needle is always towards the magnetic east but not
always towards the geographical east, while the deflexion at 2 p.m.
Jill always tend towards the magnetical west but not always
%wanls the geographical west... In fine the oscillationa hare
ir.o
reference to the nnrth niacrnetit poliofthc cartli and ml lo ihc
north Kco^n^pliical pole. No observations of this iiatun !i:iVc Wen
made in the sonthcrn heniisphere.
46. Long-Period Infqiudit Us of DfcUnaticA Hautjf. — It wa^ liiM
observed bv Lnmont tliat the yearly values ot the lUuriiai range of
magnetic deoliuatiou at iluniih niesentcj si;:pis of a lonj'-pericd
variation. In 1S52 Sabine {Vhit. Trans.^ 1&52, y. \^\ shoncd
that this inequality corrcapoiiJeJ in its process «iili that of tho
frequency of black spots on the surface of tlu- sun.
The existence of black spots on the disk of the sun wa* I0114 a;:©
known to the Cliinese. In Europe they wen lirbt srinrtihciiTy
observed after the invention of tlie telescope, and it \i33 dttluccd
from their bebaviour that tJie sun revoUis abont his axis in about
twenty-six days, liofratli Schwabo of Dessau, from 1 long s* rics of
forty ycaiV observations of the sun, was the first to show that 1I19
state of the sun's surface as reganis spots was not uniform, hut tliat
their frequency was subject to an inequality the a\ir;»f;e i»piiod ot
which was about eleven jeais. Other inequnliiirs botli of longer
and shorter periods have beeu supposed to exist, but the ehvcn-
yearly period is the Jnost prominent and is best a:>:>uicd. AilliougU
the sun-spot catalogue of Schwabe is the fn-st with preteu&iou» to
completeness, yet Professor Rudolf Wolf has endeavoured to render
observations of sun-spots made at ditferent times and by.ditlereut
observers comiwrable witli ca^h other, and has formed a list exhibit-
ing approximately the relative number of sun-spots for eacli year.
This list extends back into tbe 17tli centur}-, and is of great value
in confirming past all doubt the existence of Oie eleven-yearly jiei iuil.
It will appear below that the sun is probably to be regarded as
giving out most light and heat at those times nhcn suu-sjK>t3 aic
most frequent. The most acciirate and now universally adopted
method of estimating sun-spcts is to take the spotted area exurc£s>cd
in millionths of the sun's visible hemisphete.
To return from this digression, — the coircspondence bctveen snu-
spots and declination ranges detected by Sabine was of sucb a nature
tr.^t years of large declination range agreed with those of many suu-
rpots, and vice versa. In the same year with Sabine (185'2) Dt
Rudolf Wolf and M. Gantier independently remarked tlic same »,oia-
cideuce. Subsequent discussions have entirely confirmed the fact
of this connexion, and in May 1879 Williaju Ellis {Phil. Trnn.t.,
1830, p. 511) showed that the observations made at the Greenwich
Observatory during the years 1841-77 indicated a relation of Uiis
nature between the diurnal ranges of horizontal force as well as thoso
of magnetic declination on the oue hand and the amount of Eiin-i>j>ot
frequency on the other. The general chaimeter of tlus coincidcnca
between sun-spot frequency and declination range is exhibited
graphically in fig. 39 below.
47. Ratios of ilangcs in Years of Maximum aiia Years of iliiU-
'•miija Sun-Spot Frequency. — Broun {Trans. Roy. Sac uf Edin., voL
rxvii,) has shown that the ratios of the diunial ranges of declination
in years of maximum to those in years of minimum sun spot
frequency for places widely apart on the surface of tlie eartb arc very
nearly alike. This will be seen from the foUowiag table :—
Table VII. — Ratios cf Declination Ranges in Yeora of Maximum
and of Minimum Sun-Spot Frequency
f"" |S(S^)' «--'• 1
Paris 1 71
Gottingca 174
Munich ; 1-66
Dublin 1 1-52
Cassini aud Anga.
Gauss.
Laniont.
Llovd.
Kay.
Younghosband and I^roy.
Broun
Toronto j I'Sl
Trevandrum j 1'56
48. Closeness of Corre.tpon'ic^ice — Lagging behind of Jlangcs. —
Stewart has shown from a discussion of the declination mngcs at
Kew, Trevandrum, aud Prague (Aoc. Pinj. Soc, Hnrdi 22, 1877,
February 8, 1878, May 16, 1678) that this ccrresiwndeuce lietw^cn
the state of the suu's surface and the diurnal range of declination
extends to inequalities of shoit period as well os to tliat of nhicli
the period is approximately eleven years, but that a particular st.itc
of the sun's surface precedes in point of time that of the declination
range to which it corresponds. — in line, that the solar cnuse precedes
the terrestrial effect, which latter lags behind to an extent that i.i
sometimes considerable. These conclusions have been confrrmed by
Ellis {ut supra), and have likewise beeu extended by him to tho
horizontal force. The close nature of this correspondenre, as well
as the lagging behind of the terrestrial magnetic effect, will be seen
from fig. 35.
There oro i;-.dications that this lagging behind of the magnetic
effect is greater for sun-spot inetjualities of long than for those of
short period, a method ot behaviour quite similar to what we find
in meteorological phenomena.
49. AtuUysis of Lmg-Pcriod Inequalities. —VTe possess no snnspo*
XYL — 22
M E T EOROLOGY
170
(lata sufficiently accurate for a discussion, in a complete manner, of
questions relating to solar periodicity before the time when Schwahe
Had finally matured his system of solar observations, which was
not until the year 1832. We have, however, a much longer series
of the diuinal ranges of magnetic declination, which we have seen to
[terrestkial magnetism.
ISC
„
c
^
^
r\
IOC
r
'-A
V y
\
500
/
A
\
v
\
200
UOO
a
—
■
i\
\
'X.,
000
,S5S
lass
1800
7S„
73«
I«»3
7Sfl4
rig. 35.
follow very closely all the variations of sun-spot frequency, so it
is conceivable that they may give us a better estimate of true solar
activity than that which can be derived from the direct measure-
ment of spotted areas.
• These considerations have induced Messrs Stewart and Dodgson
to attempt an analysis of the diurnal ranges of magnetic declination,
their method being that which has been pm-sued by Baxendell and
probably other astronomers with observations of variable stars.'
The observations at their disposal for this research 'were those
which had been used 'by Professor Elias Loomis in his comparison
of the mean daily range of the magnetic declination with the
extent of the black spots on the sun [American Jounwl of Science
and Arts, vol. 1. No. cxlix.). These observations are recorded as
monthly means of diurnal declination range, and it was found
necessary to multiply each by a certain factor, first on account of
the change of declination range from one month to another, and
secondly to bring them all to the standard of the Prague observa-
tions,— Prague being the place where the longest series of such obser-
vations has been made. For this latter purpose precisely the same
corrections were applied as those made by Professor Loomis.
The result of this analysis has been to indicate the existence of
three inequalities, — two dominant ones with periods of about ten
{and a half and twelve years, and a subsidiary one mth a period of
ibout sixteen and a quarter years. By these means the obser\'ed
annual values of declination range have been reproduced with an
average error of 39". The amount of agreement between the
observed and calculated values wiU be seen from the following
diagrani (fig. 36).
' tgO. Notwithstanding the considerable amount of agreement
" r
T5-j
,.00
"77
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•'
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"
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n
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7.
!j rv
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oJ
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IS
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il^
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"ir
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ii.
Fig. 36.
>* * ' ■
fcetween tho^Tresults "of observation and calculation which appears
in the diagram, it would seem that the scries of observed values
at present obtainable is too short to render the analysis a very
accurate one.-.k It will, certainly not bear carrying back forty
or fifty years beyond its starling point, which was in 1784, and
it would be very hazardous to carry it forward any consider-
• ftoc. Lit, and Phil. Stcicty of Manelielter, Uarcb 8, 188L
able length into the future. It will be seen that calculation-
indicates a maximum of declination range about 1834, but not ao
pronounced a maximum as that of 1871. Here then we havrf a
prevision which observation will either fulfil or contradict, giving
us a practical test of the value of this analysis.
61. The remarks now made would seem at first sight to imply
that wc are not yet fumished with sufficient yearly records cither of
declination ranges or of accurate sun-spot observations to enable us
to analyse the long-period solar inequalitj' with such completenese
as to carry our calculations more than a very short distance into
the future with any chance of success, and that we may have to
wait for another hundred years* observations before we are able to
do so. On reflection, however, it would seem tlxat long-period
inequalities may bo caused by the superposition of those of short
period, and thus that an analysis of the latter may lead to that of
the former. It would relieve us if this were found tobe th6_caiie i
for the observations at our disposal may be sufficient to cnaoie us
completely to analyse short-period inequalities, assuming .that we
have in such the elements of a true periodicity.
A remark made by the authoi^s of the above analysis would seem
to indicate that a connexion of this nature between long and short
periods does in all probability exist. It is a well-known fact that
the so-called eleven-yearly oscillations of declination range are at
certain times large and at other times small. Thus, for instance
they have been large for the last forty years, but they were small
about the earlier part of the present century. Now it is clear from
an inspection of the observations (see fig. 36) that a series of large
oscillations is accompanied with an exaltation of the base line, or
line denoting average efficiency, while a series of small oscillations
is accompanied with a depression of the same. The i-esult is a
long-period curve of the base line, the Beat period, so to speak, of
the eleven-yearly inequality.
Now a phenomenon precisely similar occurs in connexion with
shorter periods. If we take inequalities having a period of three or four
months, we find that such are alternately well-developed or of large
range and badly-devcloped or of small range, ana that a large
range of such is accompanied with an exaltation of the base line or
line of avci-age efficiency, while a small range is accompanied with
a depression of the same. The result is a cui-ve of the base lint of
which the period is roughly speaking eleven years. May we not
therefore imagine that the so-called eleven-yearly period, or, to s^eak
more correctly, the ten and a half and twelve-yearly periods into
which the eleven-yearly period may perhaps be analysed, may be
in reality beat periods for shorter disturbances ? Is it not there-
fore possible that a study of these shorter periods may give us.
information regarding the natiu-e of the eleven-yearly period,'
whether for sun-spots or declination ranges, which the small series
of actual obsen'ations is incompetent to afford ? ,
52, Declination-Range Weather. — Allusion has already been
made to magnetical weather as perhaps having laws similar in some
respects to those which regulate meteorological weather- Now tlie
diurnal ranges of magnetic declinarion and those of atmospheric,
temperature present us with elements of the two weathers that can'
easily be discussed. Again there is strong evidence for supposing
that an element of meteorological weather, such, for instance, as
tempei-ature-range, travels as a rule from west to east, so that a
peculiar style of temperature-range might bo expected to appear
fijst in America and some days afterwards in Great Britain. It
becomes therefore a question for inqufry whether this travelling
from west to east applies also to magnetical weather as evidenced by,
the diurnal declination-range. Stewart is of opinion that this law
of travelling applies to both, but that magnetical weather travels
faster than meteorological (seeProc. Roy. Soc, January 10, October,
23,1879, and June 9, 1881). From the preliminary discussion made
by him it would appear that Kew lags behind Toronto as regards
phase of magnetical weather by 1 -6 days, that Prague lags behind
Kew 07 days, and that Trevandnim lags behind Kcw by 97 days,!
This conclusion cannot, however, be regarded as established untilj
it is confirmed by a more complete discussion of observations. ,
53. Disturbance. Diurnal Variation of Declination.— t^agnetie
storms (i 38) were so named by Baron Humboldt, one of the first
observers of such phenomena. From observations at Paris, Berlin/
and Freiburg he found that very frequently, though not universally,'
these three stations were simultaneously affected by sucli storms.'
The observation of magnetic disturbances was aftcrivards pursued
in a systematic manner by Gauss and Weber of Gottingcn. 'Term
days were insritutod for this i>urpose by these observers,— that is to
say, periods e.ich of twenty -four hours length during which ob-serva
tions were simultaneously made at intervals of live mmutes at
Gottingen and about twenty other stations distributed genemlly,
over the continent of Europe. Finally, the establishment by tho
British Government of the colonial magnetic observatories, and tho
energy and sagacity of their director. Sir E. Babino, have very
greatly increased our knowledge of these remarkable pheiiomona. .•
Sabine has not merely separated the disturbed from the unais-
turbed observations as explained in § 38, but ho has divided tlio
former into two categories— (1) those tending to increase westerly
TBKBESTSIAL MAGNXXISV.]
ME T E 0 R 0 L O G Y
171
declination and cither clemeat of force, aid (2) those tending to
diminish the same. He finds that t^aaa two categories obey
different laws, from which he arguaa that there are at least two sets
pf disturbing forces. In fact, if we have to give up the idea of a single
force of constant type, it is natural to ask if the phenomena of dis-
iturbance can bo approximately represented as due to the united
action of two independent types of force. It was probably some
such idea that led Sabine to separate disturbances into these two
categories above mentioned. Here there is no attempt to assert
that these two types represent an ultimate and complete analysis
of the forces concerned. We merely use the separation as the most
convenient method at our disposal in the present state of our know-
ledge for ascertaining whetner there be indications of a dual
system.
5i. }UsttU$ in the JSorthem ScTnisphere. — Sabine's method of
viewing the phenomena has enabled him to obtain the disturbance-
.diomal variation for the following stations :-
lew bV jyif. lit.
Peking 39 M K. „
Nertchinsk 51 19 N. „
Toronto « „ 43 40 N. ^
Port Kennedy „ T2 01 N. „
Point BiTTOW n 21 N. „
The above stations have been so chosen that Kcw may be
regarded as on one side and Peking and Nertchinsk as probably on
the other side of the Asiatic pole, while Toronto may ne regarded
»s on one side and Port Kennedy and Point Barrow as on the other
side of the American pole (§ 29). The q^uestion as to what
influence, if any, these poles have upon the disturbance-diumal
variation of declination is thus one which may be answered by
examining the results obtained at these various stations. For this
purpose, instead of recording the aggregate disturbances at the
various hours, the result is expressed in ratios, — the mean hourly
ratio for the day being taken as unity, or in other words the whole
N>dy of disturbances for the twenty-four hours being reckoned as
twenty-four. The results of this method are graphically represented
in fig. 37, where in the left-hand curves Kew time is used, and
in the right-hand curves local time, each starting at 0''.'
(r 8" W. long,
lie s E. „
114 9 E. „
79 0 W. „
94 20 W. .,
158 15 W. „
Kg. 37.
55. At all the various stations one curve exhibits unmistakably
a single progression, while the other exhibits more or less dis-
tinctly a double progression. At Kew, Toronto, Port Kennedy,
" If we refer to & paper by C. Cbunbeni, director of Bombay Observatory
(FA« Tram., 1868), it will be aeen that aerly distnrbancea at Bombay pre-
sent the same characteristics aa westerly ».Teldng or Nertchlnsk, the maximum
toeing aboot tweot^'-two or tweotv-tbree boiua Bombay astronomical time.
and Point Barrow it is the easterly disturbances which exhibit
this single progression ; while, on the other hand, at Peking and
Nertchinsk, stations which are oppositely related to the Asiatic
magnetic centre, it is the westerly disturbances which do so. It
is imagined by Sabine and others that tliis peculiar reversal is due
to the fact that Kew and its associated stations may be regarded as
on one side and Peking and Kertchinsk as on the other side of
the movable magnetic system.
Sabine has likewise remarked that the single-progression curves,
whether denoting easterly or westerly disturbances, exhibit maxima
which take place not far from the same absolute time. We have
therefore plotted all the left-hand curves according to Kew time,
that the eye may readily see the amount of simultaueity which their
corresponding phases exhibit It will be noticed that there is a very
striking- simultaneity between the maxima of Kew, Toronto, Peking,
and Nertchinsk, but that the maxima for Port Kennedy and Point
Barrow, while both occurring about the same time, fall at a time
decidedly if not very great^ different from that of the other
mftTiTnfl Indeed the time of maximimi for Port Kennedy and
Point Barrow is not far from the time of minimum for the other
stations. Now it has been noticed by Sabine that Port Kennedy
and Point Barrow may be regarded as on one side of the American
magnetic centre of intensity, while Toronto and the other asso-
ciated stations are on the other side. It seems therefore possible to
connect this last fact with the change in the time of maximum.
Sabine has likewise remarked that the aggregate amount of dis-
turbances is much greater at Point Barrow than at any other
station. Now Point Barrow is likewise that spot where auroras
are most frequent. Thus in the phenomena we arc now discussing
there is first of all a marked reference to the Asiatic pole ; secondly, a
reference not so marked, perhaps, to the American pole ; and thirdly,
a reference to the centre of auroral activity. Sabine, whose experi-
ence of such matters is very great, appears to think most of the
reference of these phenomena to the Asiatic pole. He thinks
that "of the two magnetic systems which are distinctly recog-
ni2able in the magnetism of the globe one has a terrestrial and
the other a cosmical source," and that it is "the latter of these
two systems which, by its progressive translation, gives rise to the
phenomena of secular change and to those magnetic cycles which
owe their origin to the operation of the secular change," con-
curring with the conclusion of "Walker that " the magnetic
influence at any point of the globe isi^e result of two distinct
magnetic systems, the principal of whitm is the magnetism proper
of the globe, having its (northern) point of greatest attraction in
the north of the American continent, whilst the weaker system
is that which results from the- magnetism induced in the earth
by cosmical action, and of which the northern point of greatest
attraction is at present in the north of the Asiatic continent. Thus
the direction of the magnet at any point results from the super-
position of these two systems, the nearest pole being always pre-
dominant over the more remote " (/"AtX Trans., 1868). 'While dis-
posed to think that something of this nature should be accepted
as a working hypothesis, we would, however, point out that the
Asiatic pole cannot be regarded as accounting for all the pheno-
mena of disturbances, but uiat the focus of disturbance is probably
nearer the focus of auroras than it is to either of the foci of
magnetic intensity.
The right-hand cunes representing these disturbance-diumal
variations which have two maxima are, except for Port Kennedy
and Point Barrow, decidedly irregular. Sabine remarks also that,
instead of having a reference to absolute time like those with one
progression, their reference is rather to local time. "We have therefore
plotted all these curves according to local time ; nevertheless this
reference does not come out with very great distinctness ; but it
must be remembered that our analysis of disturbances into easterly
and westerly, although, in the hands of Sabine, it has given us much
new information, has no claim to be regarded as final and complete.
56. Results in the Southern Bemitphere. — Table VIII. shows
the disturbance-diumal variation of declination exhibited for St
Helena, 15° 56'-7 S. lat., 6° 40'b W. long.; Cape of Good Hope,
33° 66' S. lat., 18° 28'-75 "W. long.; Hobart "Town, 42° 52' 5 .S.
lat., 147° 27'-5 E. long.
At St Helena and the Cape the easterly disturbances present the
appearance of a single progression, while the same remark slightly
modified applies to the easterly disturbances at Hobart Town. Again
the times of easterly maxima for St Helena and the Cape are very
nearly simultaneous, while Hobart Town, which we may regard as
situated on the opposite side of the chief southern magnetic centre
from St Helena and the Cape, has its maximum nearly coincident
in absolute time with the minimum of the other two stations. It
would thus seem that the chief magnetic centre of the south is
similar in its action as regards these phenomena to the chief mag-
netic centre of the north. Again the absolute time of single maxi-
mum for the south as determined by St Helena and the Cape is
about twelve hours different from the corresponding time for the
north as determined by Kew, Toronto, Peking, and Nertchinsk.
All this is in favour of the working hypothesis already mentioned-
172
METEOROLOGY'
[TERnEITriAL MAONETISJt.
Local
Aelio-
nomlco]
St Helena.
Cape of Good Hope.
HobJirt Town.
Enstcrly
Westerly
Easterly
Westerly
Easterly
Westerly
Uati03.
Hatigs.
liatlos.
Ratios.
Ratios.
0
3-24
2-46
21
1-6
114
1
317
2-39
21
1-2
1-20
3
2-79
1-68
I 11
10
1-32
071
3
200
1-44
10
0-8
4
0-89
1-29
0-S
0-7
1-39
6
0-34
0-70
0-4
OS
1-32
0-52
e
0-14
0-45
0-4 ■
0-8
1-10
0-72
7
00^
0-50
01
1-2
0C2
104
8
003
0-44
01
1-2
9
0-03
0-37
0-3
13
0'.32
•■!?
0 07
0-43
01
11
0-28
1. 66
11
0 00
0-42
0-2
0-8
0-74
i-31
13
000
0-31
0-3
0-7
0-C2
000
0-32
0-4
00
0-55
1-72
001
0-24
0-2
0-8
0C3
1-62
000
0-29
0-4
0-5
0-85
1-26
000
0-23
0-4
0-4
1-07
0-84
008
024
0-5
0-4
0-87
0-47
0-39
0-42
10
0-8
1-02
0-44
0-87
0-89
1-8
1-3
1-53
0-63
1-62
IM
2-3
1-4
1-58
0-70
2-61
1'72
2-3
1-7
1-41
8-08
2-21
2-6
1-8
1-27
2-78
200
2-7
1-7
1-24
0-62
Finally, tlio westerly disturbances at the three southern stations bear
greater marks of a double progression and of irregularity just as they
did in the northern hemisphere, and moreover like their northern
analogues they are regulated by local rather than by absolute time.
; 67. Distrihuticm of Declination Disturbance over the Various
Months of the Year. — Broun was probably the first to remark in
reducing the Makerstoun observations that the disturbances wero
greatest at the equinoxes and least at the solstices. His method
was to find for each month the mean diurnal inequality, and then
to consider the difference of each individual observation from the
monthly mean for that hour as a disturbance, the summation of all
Buch differences for the month denoting the monthly dishirbance
value. The following table embodies the results at various
Btations— those at Toronto, Hobart Town, and the Cape being
,given by Sabine, and that at Bombay by C. Chambers, who has
pursued Sabine's method of separating disturbances : —
Table IX. — Monthly Distribution of Declination Disturbances.
Jiinuary...
Mareh
ApiU
May
July..."!.'.'!!
August
September
Oetciber....
November
December.
58. A careful inspection of this table, without attempting a more
complete analysis, will, it is thought, lead to tho following con-
clusions : —
(1) Although for any station tho distribution of tho easterly dLs-
turbances over the various hours of tho day is generally difl'crcnt
Jroin that of tho westerly, yet tho same law of distribution over the
Various months of the year is followed by tho easterly and by tho
Westerly disturbances at any station— tho law at one station being,
Ihowover, different from that at another.
(2) In all stations there is first an annual inequality exhibiting
a maximum generally a short time after the summer solstice villi a
corresponding minimum for tho winter solstice, and secondly a semi-
annual inequality exhibiting a maximum generally a little after each
equinox.
(3) Tho equinox maximum is very conspicuous at Toronto; but
ixe summer maximum is most conspicuous at tho other stations.
69. In § 38 it was observed that the observations selected as dis-
ti>'bed at any station may nevertheless Iio a mixture of what may bo
termed true disturbances and of the moro prominent specimens of
taagnetic weather. Tho truth of this statement would appear to bo
■borne out by tho laws now given. In one of these wo fintf that dis-
tnrbanecs, at all stations, have a maximum about tho time of Iho
^urnmer solstice and a eorretipondiiig minimum about the tinio of the
viutur solstice, But the absolute time of tho summer solstieo for
stations north of tho equator corresponds with tliat of tho winter
solstice for stations south of the lino. It would therefore appear
that .in so far as this law is concerned such disturbances lack the
element of simultaneity. On tho other hand, a law of this nature
would naturally hold for magnetic weather. i"or at any station tho
diurnal lange of declination is greatest at the summer solstice, and
hence any considerable proportional variation of this v.-ould, if repre-
sented by a fixpd scale, present the appearance of being greatest
likewise at this time. The question thus arises whether this law
docs not rather apply to magnetic weather than to real disturbance.
Again the semiannual inerjuality of disturbance exhibits through-
out the globe a maximum at the equinoxes, and thus presents the
element of simultaneity which was wanting in the annual This
law may thercforo refer to true disturbance, and this view is sup-
ported by the fact that tho aurora — which may be regarded as tnrf
universal accompaniment of great and simultaneous d!isturbauces— •
obeys, as we shall afterwards see, in those stations whcro it ba»
b?eu well observed, this very same law, that is to say, it has lik©-
vnao maxima at the equinoxes.
60. Distribution of Decliiiation Disturbances over Various Tears.
—In 1852 Sabine discovered [Phil. Trans., 1852, p. 103) that dis-
turbances have a long-period inequality allied to that of sun-spots
in such a way that a maximum and a minimum of disturbance
coincide with a maximum and a minimum of sun-spot frequency.
This will bo seen from the following table (X.), in which we
have tho relative values of declination distm'bance at Toronto
and Hobart Town compared with the number of groups of spots
observed ou the sun's disk : —
Values of DecUnatioD Disturbance.
G roups of
Toronto.
Hobart Town.
1843
0-55
0-48
31
1844
073
0-82
62
1845
0-62
0 67
lU
1846
1-20
1-03
157
1847
1-40
1-44
257
1848
1-43
1-60
830
61. The follovriDg table (XI.) oxhibita the eame thing foi
Bombay. Tho first column of this- table is derived from thd
magnetic results of C. Cliambers, while the sun-spot areas are
those of Messrs De la Rue, Stewart, and Loewy.
Aggregate Values (in Minutes)
of Declination Disturbances.
Sun-Spot Areas.
1859
1S60
1861
1862
1863
1532-1
1421-6
951-8
1240-5
691-1
1353
1313
1297
1211
676
Wo may conclude from these tables that declination disturbances
march with sim-snots, but that tho alliance between these two
phenomena is proDably not so intimate as that between declina-
tion ranges and! sun-sjjots.
62. Distribution, of Declination Disturbances orer the Surface of
the Olobe. — It is well known that disturbances are comparatively
small near the equator, while they are great near the magnetio
poles, and greatest of all perhaps near tho position of maximum
auior.as. It we adopt Sabino's system of separating disturbed from
undisturbed observations, it is thus clear that the same sc;>aratina
value cannot be adopted at all stations. At first sight this woijil
seem to introduce an element of uncertainty in the estimation of
disturbances, but it was soon found by Sabine that no very great
nicety is required in this matter. Not only do tho laws which regu-
late disturbances at a given station remain comparatively unaffected
by the magnitude of the separating value, but it is likewise easy to
tell whether tho aggregate distm-banco value at one station is de-
cidedly greater or less than at another. Probably at present il
would be impossible to obtain moro definite infonnation tnan this,
03. Tho following table (XII.) exhibits tho proportion between
tho aggregate amount of easterly and that of westerly disturbancQi
of the decliaation at various stations in both hemispheres :—
Nome of StAtlon. Easterly. Westerly.
Toronto 140 1
Point Barrow « 1-63 ; 1
Port Kennedy _._ 1-85 : 1
Carlton Fort 1-74 : I
Kcw „ -.. 1-19 : 1
Peking 1 : I'll
Bombay »., 1*0 : 1
St Helena.. _ „ _ 1 I l-tO
Capo of Good Hope ,.» 1 : I'Al
Hobart Town 1 : 1-40
Falkland L.K« >-6« : 1
64. Annual Variation ij DecUna/ii>n.—Tht declination floctn*-
^IBBESTRIAL ItAGNSTISH.]
M E T E O R 0 L 0 G Y'
17a
lions of short period hitherto discussed are not necessarily accom-
ranted by a permanent change of mean position of tlie needle. We
tave now to inquire whether there bo any fluctuations of long
period (besides the secular change discussed in §§ 30-33) tending
^0 alter perceptibly the position of the magnetic needle. This leads
113 at once to the annual variation, for our knowledge of which we
must look to the later-made and more accurate observations, in
rwhich all possible sources of error have been carefully eliminated.
iBroun has made an exhaustive experimental inquiry into the various
sources of error which could possibly influence his declination
piecdlo at Trevandruin. His conclusion was that the variations
jof torsion of a well-made thread are not suflicient to produce a
jsensiblo effect upon the position of a powerful magnet. In fact
JGnibb's magnet, weighing 6000 grains, and Adie's, weighing 1100
grains, give almost identical results. Wo may extend these con-
clusions to other observatories where well-devised instruments have
teen established, and look with much confidence to such instru-
ments registering correctly the secular as well as the annual
change of declination that may be taking place at each locality.
65. The following table (XIII.), borrowed, with the exception of
the Trcvandrum and Bombay results, from E. Walker's Terrestrial
Hcuftutisin, shows tlic annual variation at seven stations; —
Hobai-t Town.
M llelrna.....
The C.-ipe
Toronto
TierunJrum.,
bombay
21 39 W.
0 seE.
23 37 W.
29 7 W.
1 35 W.
0 35 E.
0 31 U.
7 39 00 E.
1 2320 W.
7 57-00 W.
0 23<0 W.
1 5712 W.
1 35-4 E.
3 10 E.
1858-S2
18M-18
1841-49
1841-46
1815-il
1854-69
1859-65
^Table XIV, — Showing the Mea% Anntuil Variation for cacJt
Month of tilt Year at Seven Statiorts.
*
1
S
i
5o
1
1
Trerondrum.
1 B
Grubb. Adie. »
4- 1-5
-41-8
-ior,
-70-3
-20-7
4- 9-8
4-40-6
+343
4-390
4- ili
4-31-2
4-29-8
- 0-0
- 9-6
-17-4
-42-6
- 4-2
4-47-4
4-i;i-o
4- ■-■1-6
4-19-8
4- 4-2
4- 0-6
- 7-S
- 2-4
- 1-2
-13-8
4- 8-4
- 3-6
-19-9
4- 1-8
4- 7-2
4- 7-2
- 30
4-18-0
4-10-2
4-64-2
-10-8
-02-4
-22-2
-38-7
-24-1
4- 1-2 4- 6-3 1 4-11-0 !
4- 3-4 4- 8-7 4.16-3,
+ 5-6 4-8-7 4- 9-8 j
4- 1-6 4- 2-2 1 4- 1-7 1
- 2-8 -3-2,4- 1-6,
- 8-7 -10-5 14-0-4,
- 80 -111 1-8-9
4- 1-2-30' + 1-2
4- 3-3 - 1-3 -18-2 1
4-7-14- 3-2: -10-9 I
4-2-3 4- 2-0 14-3-11
- 4-9 - 1-2 - 7-0 i
May
-61-8 -1-2-.'
-43-2 , - 4-5
- 4-8 4-136
4--i5-2 1 4-27-6
4-4-2-0 1 4-3S-.i
September.,...
October
KovcmlKT.
Uct'Cmbcr.
Febiaiiy-
March
4-43-2
4-49-8
4- 7-9
4-10-7
Here 4- indicates that the marked pole of the needle is to the
west and — that it is to the cast of its mean position for the year.
60. To cancel the in-egularitics of this tabic let us take the means
from Api-il to September and from October to "March, the former
embracing tho itioiiths around the Juno solstice and the latter
(hose around the Dcceiubcr sojstice (Table XV.): —
i
.Mentis from
Means Troin
April to September.
October to March.
Kcw
-28-7
4-31-8
Toi-oiito
- 4-.'>
St Iklroii
- 6-4
CniH of Gi>nd Hope
-29-7
4-30-9
-18-7
4-17-3
TrcvanJrum
4- 2-1
- 1 6
Bombay
4- 0-3
- 6-8
It will be seen from the ahove that the means for Trcvandrum and
BoKibay present opposite signs to those for the other stations. The
wb.>le amount for Trcvandrum is no doubt very small, and
Ciiainbers does not regard the evidence for Bombay as conclusive;
out on the whole it would appe.-vr that two observatories near
one auotl'.er present evidence of a similar behaviour in .declination,
and wo are therefore disposed to regard it as a reality.
67. Si-miannuat Variation of Declination.— If we look at
tho numbers of Table XIV., we shall see that theio are traces
of turning points at tho equinoxes. Let us, in order to exliibit
this, compare together the sums for the six months grouped
around the two equi'lMxes with those for the six months groujied
around the two sobtices — that is t-j say, compare tho sums for
Fcbnnry, March, April, August, September, October, with those
for November, December, January, May, Juno. J>il»— »nd wSLthus
«htun the following Ubie ^XVL)--
Kew
Toronto
St Helena
Cape
Hobart Town .
Tl-evandrum ...
Bombay
Sums around
S
r.16 nroiuid
Equinoctial Months,
Eolstillul Mentha.
4-104-2
-M-7
4- 90-4
-21-0
4- 4-S
4- 4-8
4- 47-4
-34-2
- 0-7
4-25-6
■+20-3
4- 0-2
- 0-1
68. Solar-Diurnal VaricUions of the Horizontal and Vertical Com-
ponents of Magnetic Force. — Although self-recording niagnetogiajihs
have bceu established in many observatories tluou^hout the glooe,
yet, owing to tho peculiar difficulties of the task, and the labour of
the process of reduction, very little has been done tow ards determin-
ing tho solar-diurual variatiou of thehomontal and vertical codi]k>u-
ents of the earth's magnetic force. Senhor Capello of the Lisboa
Observatory has, however, made progress with nis reductions, and
has already published valuable mfomiation regarding the solar*
diurnal fluctuation of the t\vo force elements at his obsci-vatory.
In his atteuipts to eliminate tlie disturbances of horizontal and
vertical force by the method of Sir E. Sabine, Senhor Cajicllo has
experienced considerabledifficulty, more particularly with the records
of the vertical force magnctogranh. Tliis instrument and tho
bifilar have very often been found by him to change tlieir position
of equilibrium after strong perturbations. Again there is generally,
for any houi', a variation at the beginning and end of tho month
from the monthly normal value for that hour owing to uhangc o!
temperature, and this cannot be completely corrected inasmuch aa
the coefficient of temperature is not exactly known. These two
causes combined tend to falsify the results when the plan adopted is
the method of comparison between the individual values of any hour
and the normal monthly average of that hour. Senhor Capello ha?
found it necessary to selert and extract the disturbances, not
directly from the hourly values, but by comparing the variation of
an individual day with the average diurnal vaiiation derived from
the month.
To illustrate this method by means of an example, let us imagine
that the sum of the t\venty-four hourly values for a particular dLy
is 24,000, and that the average monthly diurnal variation would
indicate that a particular hour of this dayshoiUd have a value 990,
then, if the value for this hour should prove to be gicatur or less
than 990 by more than a certain amount, it wotdd be set aside as a
distui'bed observation. Senhor Cajjello rather thinks it will be
desirable somewhat to modify this method, and he concludes his
remarks by observing that for t)iis and other similar questions
it is most necessary that directors of establishments possessing
magnetographs should agree together to employ the same mcthuu
in their reductions in older that their results may be compar-
able with each other. With the view of adding weight to these
remarks, we may quote the obscn-ation of Sir William Tlionison,
that our ability to analyse mathematically that influence which
produces tlie diurnal variation will depend upon our knowing
at a certain number of stations the exact iiatuic of this diur-
nal variation for eaeli of tho three magnetic ch-mcnts. A complete
theory of this diurnal influence must therefore wait upon tlio
concerted action of the directors of the various establishments
possessing magnetographs.
69. Change Cn Horizontal Force Range froTn Month to Month. — ■'
Although we do not possess finally accurate detcrininations of the
solar-diurnal variations of either clement of tlje force, vet wo are in
))Ossession of information regarding the change in the iliurnul range
of the horizontal force from month to month at the Greenwich
Observatory. William Ellis has given us the Ibllowiiig table
[Phil. Trans., 1830) representing the monthly mean diurnal rungcof
horizontal force at that observatoi-y expressed in tc-n-thousandtlia
of tlie whole horizontal force. In tlie formation of thcso jneatis,
days of great inagnctic disturbance were rejected, and also certain
other days on which there prevailed a .smaller but considcrablo
£ mount of disturbance estimated according to a gunci-al utaudard
formed in tlie examination of many thousands of jdiotograidis.
Table XVII. — Monthly Mean, Diurnal Range of Uvrizontal Force
at Royal Observatory^ Orcemoich.
Thus, like tho dotlination range (§ 43), the hoiizontal force range
has a maximuin in stunnier and a niinimiuu in winter, and cxhibita-
a tendency towards maxima at the equinoxes.
70. Long- Period Tncqnnlitics of Horizontal Force JCange.- .
^9fring Behind.^ — Ellis has com]>arcd the diurnal rango of tho'
horizontal force as wcU as that of the declination at Greenwich
with the i»eriod of sun-sjtot frequency, his cunijaiisonH extending
from 1841 to 1877, and he has deduced tlie following conchisions:—
> Secchl (Wolfs AUronrtVilsrbe MittheUumjen, No. 21) «-vm."i lo Iiuvc been iho
Bret vt ln<lli-aic a rcl.-iiton lK*i>«ucn Uio ttotc of tbc aun's Butfioc mud Die diuriutl'
TarUttoa In tbu hoiizuiital force.
174
METEOROLOGY
[tERUESTBIAL MAGNETISIt.
(1) Tlic diurnal ranges of the magnetic elements of declination
anil horizontal force are subject to a periodical variation, the
duration of which is equal to that of the known eleven-year sun-
spot period.
(2) Tho epochs of minimum an^ maximum of magnetic and sun-
spot effect arc nearly coincident, tho magnetic epochs on the whole
occurring somewhat later than the corresponding sun-spot epochs.
The variations of duration in difl'orent jjcriods appear to be similar
for both phenomena.
(3) The occasional more sudden outbursts of magnetic and sun-
spot energy, extending sometimes over periods of several months,
npiiear to occur nearly simultaneously, and progress collaterally.
71. Disturbance Diurnal Variation of Force Components.— Ifa
may derive the following conclusions from tho results obtained by
S;ibino for tho observatories of Toronto, Kew, and St Helena. For
fach element there are two categories, namely, those disturbances
v.'hicli tend to increase and those which tend to diminish the
cifMicnt in question.
(1) At Toronto the disturbances increasing both elements of force
well represent single progressions with maxima occuiring for both
about 4 or 5 hours local time. Again the disturbances decreasing
bcih elements represent fairly well single progiessions with maxima
occurring for both at about 14 or 15 hours local time.
(2) At Kew the disturbances increasing both elements represent
well single progressions with maxima occurring for both about 5
houi-s local time. On the other hand, the dirturbances decreasing
the horizontal force represent signs of a double progi-ession and
those decreasing the vertical force signs of a single progression, the
maximum for tho latter falling between the two maxima for tho
former, and occurring at 14 hours local time.
(3) There is not the same close correspondence between the
progi'ess of the disturbances wliich tend to increase both elements
Hor between the progress of those which tend to decrease both
elements at St Helena as there is for the other stations, nor is there
the same likeness between the numbers for St Helena and those of
Toronto or Kew as there is between tlie numbers of Toronto and
those of Kew.
72. The fact that the disturbance-diurnal variations of the two
force elements at Kew are very like each other while neither of
Table XVIII. — Hourly Ratios and Frequency of the Kew Peals
and Hollows, the Vertical Force Disturbance being taken at
Unity.'
Hour.
L'ncM.
llor.
Number of
near '^""■
nor.
Xumbor of
naciun.
Furcc.
Obseiratlons.
Force.
Ob-ciTatlonil.
0- 1
2-14
206
12-13
1-70
2-68
3
1- 2
1-97
218
13-14
2-00
2 04
3
2- 3
l-SO
1-90
11
14-15
2-10
2-14
5
3- 4
1-81
2-0.'.
15-10
2 -05
2-11
10
4- 9
1-3S
1-73
1(1-17
3-48
2-16
IS
0- G
1-67
171
17-18
3-80
2-14
22
6- 7
18-19
3-94
2-18
2S
7-8
1-62
1-91
19-20
3-97
2-25
2t
8- 9
1-60
2-20
20-21
3-41
221
23
9-10
0
21--i2
3-20
2-30
16
JO-U
1-33
3-15
1
22-23' 2-;9
2 00
10
11-12
1-30
2-32
3
23-24 2-.';0
204
U
74. It will be seen ifom tins table that the ratio between simul-
taneous peaks and hollows of the two components of the force is very
nearly constant, the horizontal force disturbance being about double
that of the vertical force, so far as size on the curve is conccnicd.
It will also be seen that there is a very marked diurnal range in
the ratio which the declination peak or hollow bears to that of the
vertical force, this ratio being greatest about 7 a.m. About this
hour we have also most peaks and hollows, while in the evening and
early inorniiig hoiu's there is so great an absence of these phenomena
that the ratios are doubtful.
75. A preliminary comparison between the peaks and hollows
at Lisbon and at Kew has been made by Capello and Stewart
(Proc. Ho!/. Soc, January 28, 1864) with the following conclusions.
(1) The Kew i>eaks and hollows are simultaneously produced at
Lisbon in all the elements, but to a smaller extent than at Kew.
(2) The direction is the same at both stations for the declination
and horizontal force peaks and hollows, but it is reversed in the case
of the vertical force, so that a sudden small increase of vertical force
at Kew corresponds to a diminution of the same at Lisbon.
It would be manifestly impossible to discuss with any advantage
the nature and origin of these peculiar changes until raoi-c exten-
observatlons of them have been made. As the peak and
them is very like the corresponding declination variation (§ 54) | i^q^^^^ foj-ce is probably of a simrile nature, a'further knowledge of
receives confirmation from a visual inspection of tho Kew curves.
In the Philosophical Transactions for 1862 Stewart thus describes
the result of an inspection of the disturbances of these curves for
the years 1858, 1859, 1860 (distxirbance years) :—
"There nre twenty-two cases in which the declination is raised or lowered
along witli the horizontal foice, and only seven cases of an opposite description.
Also there are twenty-two cases in wliioh the declination is raised or lowered
along with tlio vertical force, and only eleven casca of an opposite description.
Finally, there are thirty-one cases in which both forces arc raised or lowered
tocether, and only two cases of an opposite description, Tiiere is theiefore a
decided tendency in the carves of ail the elements to be raised or lowered simul-
taneously, but this tendency is stronger between the horizontal and vertical force
curves than between either of these and the declination. It may at the same
time be affirmed that with the exception of tlie disturbance of August to Septem-
ber lSo9 there is no very prominent case in which the three elements do not rise
or fall together."
73. Peaks and Hollows. — These are certain small but abrupt mag-
netic changes which from the fact that they generally fall within
the separating value are not usually regarded as disturbances. Those
changes can only be brought to light where there is a continuous
record of magnetic phenomena nuch as that derived from self-
recording magnetographs. They were first studied at the Kew
Observatory by StewaYt {Phil. Trails.^ 1862). "We have seen that
more than one type of force must be concerned in producing
magnetic disturbao^as. This is confirmed by the appearance of the
Kew records, from which it may be seen that no disturbance of any
nwgnitude is due to the action of a single force varying merely in
if&rount but not in direction. For if there were only one typo of
force the distance at any moment of a point in the curve of one
of the elements from its normal position should bear throughout a
disturbance an invariable proportion to the distance of a correspond-
ing poi/it in the curve of another of the elements from its nownal;
but this is by no means the case.
But even if several independent forces are at work it may be
thought unlikely that at the same Inoment a sudden change should
take place in all ; there is thus a probability that sudden changes
of force, as exhibited in peaks and hollows, are changes in one of
the elementary forces concerned. Even if tho change is not a very
abrupt one, prortded that wc confine ourselves to such peaks and
hollows as present a similar appearance for all tho curves, wo may
suppose that we are observing changes in one only of the elementary
disturbing forces ; for it is unlikely that two or more independent
forces, changing independently, should nroduce similar appearances
in all of tho three curves.
Assuming it as probabio that similarity of appearance in the
curve variations of the three elcmonta denotes a simplicity in tho
disturbing foico, Stewart has discussed all such peaks and hollows
at Kow c-^tending over the first two years of their production, and
has obtained a result which is embodied in the following tabic; —
its character may be of much importance to the theory of tciTestrial
magnetism.
It is interesting to remark that we have in peaks and hollows the
same close relation between the variations of the two force elements
that we find in the larger disturbances.
It is believed too that during violent disturbances a certain
change of type is produced in the peak and hollow force, and more
especially is this remarkable in the great disturbance in August and
September 1859, where the declination would seem to march in the
Opposite direction from the two components of the force. "VVe have
seen that the same peculiarity characterized on this occasion the
larger and more apparent magnetic changes. AVe shall afterwards
refer to a circumstance whidi may perhaps throw light upon this
peculiarity (g 93), meanwhile wo conclude by again remarking that
duiing comparative magnetic calms the peak and hollow force shows
signs of remaining constant in' type, and that it is therefore of
great importance that the directors of observatories possessing self-
recording magnetographs should take united action to observe this
force.
76. Oilier Inequalities of the DislurhancC'Diurnal Variation of the
Force Comjsoitcn^. ^Sabine has shown that disturbances of the force
components present a distribution over the various months of the
year very similar on the whole to that which is exhibited by «.lis-
turbances of declination. He has likewise shown that disturbances
of the force components present a distribution over various years
similar to that exhibited by disturbances of declination. Finally,
we may probably conclude that disturbances of the force comrionents
are smallest at-those portions of the earth's surface where disturb-
ances of the declination are smallest, and largest at those portions
where such disturbances arc largest.
77. Annxtal and Semiannual Variation of Horizontal Force and
Dip.~-^TQ\xn {Trans. Roy. Soc. Edin. for 1861) has discussed the
results obtained by Sabine at his magnetical stations, and has shown
that differential and absolute observations agree in telling us that
tha horizontal force is smallest at the equinoxes and greatest at
the solstices. "Whipple has recently obtained the same result from
the Kew observations.
We have deduced the following table (XIX.) from the various
absolute determinations that have been maiU- at sundry places. lu
it the annual and semiannual variations of declination, horizontal
force, and dip are exhibited, "increase" denoting a push to the
west, and " decrease" a push to the east. The metnodif obtaining
these has already been indicated in §§ 66, 67.
It, and a hollow of one cleiacnt to a hollotr of another.
^EBRBSieiAL MAOXETISM.]
METEOEOLOGY
175
Makenrtoun or Kew
Toitnito IncrcAse.
Cape of Good Hopp i Increase.
HobartTuwn _ __ T)<u.wa..>
Effect on Declination.
At June Solstice
compared to
December Soiatice.
Decrease.
Decrease.
Decrease.
Increase.
Decrease.
Effect UD HorlzoDUl Foi-<
Decrease.
Decrease.
Decrease.
Decrease.
At June Solstice
compared to
December Solstice.
Increase.
Increase.
Decrease.
78. In discussing the results of this table we shall assume that
the son acts, and in all probability acts indirectly, upon the
magnetic system of the earth. This point will afterwards be
further examined. Meanwhile, assuming this indirect action of the
siin, and assuming, to fix our thoughts, that it is in close alliance
with the convection system of the earth's atmosphere, wo can readily
imagine that such solar action would act most strongly on the
earth's magnetic poles at the solstices, and that in the June solstice
the pole or poles in the northern hemisphere and in the December
solstice those in the southern hemisphere would he most affected.
Now a strong action of this kind upon either magnetic pole may
wcU be presumed to increase the general magnetism of the earth, or
at least that portion of it which is most readily aflected by external
action, that is to saj-, the induction system. Again, if the solar
magnetic influence is connected with the convection currents of the
earth, we can readily imagine that the influence in the northern
hemisphere where there is much land should exceed that in the
southern hemisphere where there is much water.
If these views bo reasonable we might expect two things to
follow:— (1) the earth's induction system should be stronger at the
solsticfs than ac the equinoxes, and (2) it should be more especially
strong at the June solstice, when the sun acts in the northern hemi-
sphere. We must bear in mind, however, that so vast is the
sarth that a stimulus applied to its particles most susceptible of
magnetism may not be instantaneously propagated throughout
its mass, but that time may enter as an element of the question
in which case, inasmuch as the action of the sun at the June solstice
IS m the northern hemisphere, a station near the south pole may not
folly partake of the magnetic efi'ects of this action.
79. An hypothesis of this natiu-e would appear to be consistent
with the results of Table XIX.
In the first place, if the earth should become stionger as a magnet
in one or m both of its magnetic systems this would" show itself by
an increase of horizontal force at least in aU such stations as those
at which absolute observations are made. An influence which
mereases the horizontal force at these various stations is therefore
naturally regarded, and was regarded by Broun, as one increasing
the strength of one or both of the magnetic systems of the earth—
whether of one or of both wiU presently appear. We may therefore
assiune from our observations that one or both of the earth's mag-
netic systems are strongest at the solstices. •
■ In the next place we may imagine that the changes of declination
and dip which the table exhibits as occurring at the solstices aie
the very changes whicli would be wrought in these elements by an
increase of power in the earth. For we see very weU that an
increase of horizontal force at the va-.^ous stations may be regarded
as denoting an increase of the earth'i magnetic power. We cannot
however, see with equal facility what changes would be produced in
the declination and dip by an increase in power of one or both of
the magnetic systems; but we may weU imagine that such changes
ot these elements as are found to accompany an increase of horizon-
tal force are those that denote an increase of the earth's power
■ We have thus ascertained the probable nature of those changes of
the three elements which denote an increase of power. Now it will
be noteed from the table that the cflect at the June as compared
mth That at the December solstice is of the opposite nature to the
eflect at the equinoxes as compared with the solstices, —that is to
say, the earth is more powerfully affected in June than in December
the only well-estabUshed exception to this being Hobart Town in the
far south. But, assuming that time is an element in the develop-
ment of thispreponderating influence acting in the north, it is easy
to see why Hobart Town should not exhibit its full efl-ect.
Jl_ It remains to determine from the observations themselves which
of tiie magnetic systems it is that exhibits these oscillations.
Analogy would of course point to the induction system, but it is
desirable to determine this from the observations themsdves. •
I In § 5i, when discussing the disturbaiice-diurnal variation of
decUnation, it was found that Toronto and Kew may be regarded as
on one side of the Siberian pole, while Peking, Nertchinsk, and
Bombay are on the other. Now, if it be this pole that is influenced
by the oscillations under discussion, we might expect thattlie influ'
enco on declination at Toronto and Kew should Ibe the opposite of
that at Trevandrum and Bombay. We find by the table that this
IS the case, and wo are thus inclined to attribute these changes to
the biberian utetcad of the American polo. ^It would thus appear
At June Solstice
compared to
December Solstice.
that the observations of Table XIX. bear out the provisional workins
hyuothesis which we have ventured to introduce. It is quite nos
aible that these remarks may not stand the test of more comnleto
inquiry, but they are here introduced rather as denoting a method
of looking at the subject which ought we think to be pureued than
as embodying conclusions of a final nature.
80. Effect of tlie Slate of the Sun's Surface upon t/u Absolute
Magnetum of the Earth.— We have now to consider whether the
state of the sun's surface permanently influences the magnetism of
the earth. It will at once be seen that any such action will appar-
entlymanifest itself as an oscillation in the secular change. We must,
however, carefully guard ourselves against prematurely concluding
that It implies a variation in the amoimt of true seciUar change.
There may be tivo distinct things— true secular change due to que
cause, and action depending on sun-spots due to another. These,
from the nature of the case, are necessarily mixed up together in the
yearly changes which we examine; it does no't, however, follow that
there is any real identity between them. We shall now give one
example of the method to bo pursued in the attempt to detect a 'olar
influence of this nature. Let us turn to Table III., and tafce the decli-
nation yearly values at Toronto from 1856 to 1871. Subteicting the
value for 1856 from that for 1871, we find that the westerly declina-
tion had increased in fifteen years 51'-6, that is to say, at the mean
rate of 3'-ii per annum. Again, the average declination for the
sixteen years 1856-71 is 2° 20'-8 corresponding to the epoch ai
the commencement of the year 1864. Taking the aveiage value and
epoch, and also the average yearly increase above given, we are able
to construct the following table (XX.), in which calculated and
observed values at Toronto are compared together :
Observed.
Calculated.
Difference.
1856
1 5G-30
1 55-00
2 0-50
1 58-44
2 1-88
-I-2-08
1 1000
2 8-76
2 14-40
2 12-20
2 15-70
2 15-64
2 1910
2 1908
2 21-90
2 22-52
2 24-80
2 25-96
2 27-60
2 29-40
2 29-80
2 32-84
2 33-20
2 86-28
2 3710
2 39-72
2 41-90
2 43 16
2 4790
2 46-60
-i-1-30
It may be gathered from this table that the years which corre-
spond to mmunum sun-spots have in the last column a greater
negative or lower positive sign than those which correspond to
maximum sun-spots, and hence we may conclude that at Toronto the
tendency of many sun-snots is to increase the westerly declination.
81. Performing a similar operation for all those cases in which we
have a sufficiently extensive series of observations to work upon we
obtain the following table : —
Table XSI.—Sfect of Numerous Sun-Spots onTiheHFaitles' of
Magnetic Elements.
Station.
Declinaiion.
Horizontal Force,
Dip.
Kew
Increase.
Increase.
Increa&e (?),
Decrease.
Increase.
Inappreciable.
Increase.
Uncertain.
Increase.
Cape of Good Hope
82. We have good gi-ounds for supposing that the sun is most
powerful when there are numerous spots on his s-irface, and therefore
the above table represents a state of things which we may imagine
to be caused in one way or another by increased solar power. Now
the most natural hj-pothesis is to imagine that an increase of spots
acts in producing an increase of disturbances, and that for those
stations at which the disturbances tend on the whole to afl"ect the
elements in a definite direction there will be left behind a permanent
effect in this direction. A comparison of Table XXI. with Table
XII. wiU, 'however, show that this explanation is not valid. For
instance, at Toronto and Kew disturbances tend rather to diminisli
ns
METEOROLOGY
^rEREESTIUAL MAGNETISM..
cf .li
to increase the westerly declination, ^iliile the effect of numcr- I same directi..n U-r.j.e ihi. curve tumcil. Thi5 more gn-lii.-il c^n--
pots IS to increase it. Again, at the Cape the tenJcncy tinuation of the first su'lden movement lastcU about Bevcn roinute»
< is to increase the westerly declination, while that of
numerous sun spots is to decrease it. At Trevandruni again (if we
judge of it 1)1 IJomhay) the effect of disturbances will be to increase
the easterly di i Hnation, while that of suil-sj.ots is to decrease it.
Again, it is lulicve.! that at Kew and Toronto the supposed disturb-
ance effect on the dip agrees in character with the sun-spot effect.
On the whole, therefore, there is no definite relation between the
I im effects.
Now if we take Hobart Town, the Cape, and Trevandruin in the
ariove table, we find from Table XIX. that these stations seem
t.i indicate that the magnetic state of the earth is mo^t powerful
at times of niaiiimum sunsjKJts. Kew and Toronto, however,
so far as declination and dip are concerned, apiiear to go the
other way. If, however, we suppose that during the several
Mara of ijiaxiinnni sun-spots the American pole as well as the
■Siberian is affected, and tliat on such occasions of long continuance
the former has more inlluence than the latter, we shall be able to
reconcile our results with the hypothesis of increased solar action.
We can understand too that time must be au important element in
anyilillucncc coniinnnicated to the American pole, and that, although
such intlucnce might be ai.parent at Toronto and Kew, which are
eoinparatively near the pole, it would not be appareut at the other
stations of Table XXI. We .shall recur to this subject wheu dis
cussing secular diaiige.
Vaeiou.s Vhexomexa connected with the Scs and with
Tekrestp.i.iil Magnetism.
83. Ctosciu^ss in Tiiiu between Solar Changes and Magnetic
Vislurlxi lias. — Loomis (American Journal of Science, vol. I.)
has registered the extent of sun-spots for the six days preceding
and following each of the great magnetic disturbances at Greeii-
with, and has compared these values with that for tho very
Jay of the disturbance. lu this manner he has treated all the days
of great magnetic disturbance at Greenwich for a period of twenty-
three years, with tlie exception of those cases in which very few
observations of suu-spots were made. The cases of disturljance
thua treated amount to one hundred and thirty-five, and t!i5
fpUomug result lia.s been obtaiucd; —
Table XXll.—ExteiU of SiioUcd Solar Surface.
Days before Storm. Storm. Days after Storra.
664321 1234SC
las°^jl. }*'■' '">' ^'^ ^^'^ *2'' ■"■' "■' ^5-0 45-1 49-3 45-6 452 45 3
From this result Loomis draws the following conclusions: —
(1) great disturbances of the earth's magnetism are accompanied
by. unusual disturbances of the sun's surface on the very day
of the magnetic storm ; (2) the great disturbance of the sun's surface
which accompanies a terresvrial magnetic storm is generally heralded
by a smaller distm-bance three or four days previous, succeeded
by a comparative calm which immediately precedes the mngnctic
storm.
84. There is one instance on record of a sudden solar change
which was practically simultaneous with a magnetic disturbance.^
On September 1, 1859, a little before noon, R. C. Carringtoii
was observing by means of a telescope a large sun-spot, when, to
*luote his own words —
f " WIttiln the area of the great tioilh irronp (the size ol whlcli had previously
exciteil general rcm.irk) two patches of inlensely bil^-ht End white light broke
out. ... I noted down the time by the chronometer, und, seeing the outburst
to be very rupiilly on the increase, and belnff somewhat flurried by the suitiHsc,
I hastily ran to call some one to witness the cxiilbition with me, and on returning
within sixty seconds was mortified to find that it was alix;o<ty much clinngcd and
enfeebled. Very shortly afterwords the last trace was gone; and, altliough I
maintained a strict watch for nearly an hour, no lecurrcnce took place. . . . The
Instant of tho flR»t outburst was not fifteen seconds different from ll*" 18"» Green-
wich mean time, and IIi" 23"i was taken for tho time of disappearance. In this
lap^c of five minutes, the two patches of light traversed u space of about 35.000
miles. ... It was impossible, on flist witnessing an appearance so similar to a
Buddcn conflagration, not to expect a considerable rvsult In the way tff alteration
of the detiills of the group in wliich it occuircd ; and 1 was certainly si'irpi Iscd.
on referring 10 the sketch which I had carefully and satisfactorily finished before
tho occurrence, nt flnding myself iinablo to recognize any change whatever as
having taken place. The impression left upon me is that the phenomenon took
place at an elevation considerably above the general surface of the sun, and
accordingly altogether above and over the great group in which It was seen pro-
jected.
* It lias been '
observing the
a of what ho also considered a
t Mr Hodgson ciianccd to be
me duy. and to hear that he
arkable phenomenon."
observed this plieno-
' nultaneotisly
At the very moment when Carringtoii
menon titc three magnetic elements at Ki
disturbed. Tliis disturbance occurred as nearly as possible at
llt» 15ra X.M., affecting all tho elements simultaneously, and
commencing quite abruptly. The first or most abrupt portion of
tho disturbance lasted only about three minutes for all the
dements ; but after tliat thero was d more gradual chaiigo in tlio
> eM- lynu, Mgrualwr SI, leCI,;
for all the elements. This m.ignelic disturbance was, however,
in reality a small one, and nas followed by a very great uLiturbance
whidi took place not many hourx afterwards.
85. Simiillancili/ of Changes of llori-.emlal Force at Varicus Parts
of the Earth.— \\t have alre^sdy (| 79) alluded to tlie superiority
of the horizontal force in indicating by its changes what is taking
place in the magnetic system of the earth. If this system bo
strengthened as a whole we shall no doubt 11m', the horizontal force
increased in value at our various stations, while if the earth's powei
be weakened as a whole we shall find the hori.'ontal force diminished.
Broun has discussed this subject at gre.it length in a. memoir
alicady mentioned, and has embodied liis observations in numerical
resuUs from wliich the following table has been extracted:—
Table XXIII.— JPnt/i/ Means of Horiioiilal Force at Makcrslaun'
(XI.), Trevandruin (T.), Singajiorc (S.), and Hobart Tcu-n (H.).
1844.
M. , T. 1 S. 1 H.
1844. 1 M. 1 T. 1 s. 1 n. ]
M
arch 1
21-40 1 07-42
lC-40 IC-4G
March 17 2130 H-M 1 19-74
1912
8
18 34 1 0.V25
1418 13-98
„ 18 2011 07-62
17 -C5
1-03
,, 4
10 53, 0042
H'59 14-49
„ 19 21-73 03-55
16-26
K 59
„ 5
0f4.J
1279 10-04
„ 20 -2200 07-83
17-21
01-85
10-42 1 9-CI!
„ 51 23-15 09-00
18-35
17L^
'
1239
0412
12-37
9-98
„ 22 22-47 1 08-14
18-35
lo-l:
8
10-94
03-81
I3-G2
11-50
„ 24 , 22-30 1 09-5S
18-76
.. 10
1012
04-33
14-87
14-07
„ 25 1 -iS-Tl , 1009
18-76
M "
17-M
05-87
I4-S7
13-97
„ 26 1 25-22 09-48
20-29
„ 12
lS-05
06-28
15-01
14-22
,. 27 1 22-24 10-81
18-63
„ 13
23-25
09-58
17-65
16-18
„ 23 22-10 07-52
17-79
ii;.73
,p 14
23HC
lOCl
18-90
17-81
„ 29 -5-97 03-50
11 -,•,4
„ 15
2212
1009
1603
lC-85
„ 31 1700 02-27 II-SI
10-27
This table shows a considerable likeness between the daily changes
of the horizontal force at the four stations. For instance, we have
a niininiura which occurs on ilaich 5 at Makei-stoun and March ft
at the other stations ; we have likeivise a well-defined maximum
occurring at all stations on March 14, and another occurring at
Trevandrum on March 25, and at the other stations on March 26.
Finally we have a well-defined minimum occurring at Trevandruu:
on Marcli 31, and at the other stations a day earlier.
Broun has extended a similar tixatment to daily means for
every hour, and fig. 33 conveys a good idea of the amount of sioml-
taneity which obtains in the changes of such values of horizontal
force at stations far apart.
86. Mccurrciicc of Disturbances at Intcnnls of about Ticentij-six
Days. — Broun- and likewise Horustein^ have observed that there is
a tendency in large magnetic changes to recur at inten'als of about
twenty-six days. At first it was natural to suppose that wc have
here a ma^netical indication of the true time of the sun's synodical
rotation, tlie interval between two disturbances denoting that wliich
elapses between two presentations to the eartli of a peculiarly
powerful solar meridian. It seems unlikely, however, tliat there ia
a really permanent one-sidedness of this kind in onr luminary; but
the result of observation seems to show that for a limited period,
say two or three years, certaiu meiidiaiis of the sun appear to be
peculiarly powerful. The cause of this we shall not here discuss,
but simply treat the phenomenon as a fact derived from observation.
Broun m liis paper above quoted (Phil. Trans.y 1876) makes the
following remarks : —
" Wc haTo seen that %vhcn one side of the tun Is presented to the Mrtli lh«
magnetic foice o( the latter Is greater than when llic other side Is tu^-ncd towards
ua; we may even my that the Intensity Is jrrealcst for a pivcn fcojar ccvldlsn;
this, however, may be simply an Integral effect resulting from the action du« ta
all the meridians. But can we eupp.isc when a preat und sudden Incrusc or
diminution of Ihc earth a magnetic force occui-s that ihls Is produced Ijr aome
change oecurriog oD a partiiuliir Bolar lUcrldLaD? This docs Dot seem at all
improbable.
*• In order to examine the facts, all the eases were noted durlnic the yean l&H
and 1^5 ill which the dally mean hoiisontal torcc dimlnt»hed onc-thousiindrtt oC
Us whole value within an Interval of three days; they were found to be twcnly-
elK'it In numbvr. If we call the solar meridian presented lo us pn the 1st January
Id-M the zero meridian (0), and con^dcr the time of rotaiton to be twtnty-alx
days, and that there ore twenty. six mt-rldlnns. wc flnd that the sol ir meildlans
presented to us wlu-n thcac gicat niovcmc "is occurred may be an^nged In a few-
groups, as In the following tiiblc" [Tt^lc XXIV.. p. 177]. -
" An examination," continues Droun, " of this taMe will show that nearly half
of the great chanjicj began when the eighth mirldijn alter the xeio had [vuscd.
while five begun near the t»clfili after, and Arc near the lero itb*tf. ... If
any douU existed as to Ihc possibility of lhc>c Ulng mere accidental colncldcncei^
It would bo rem-vcd. t think, by a consideration of the marked aucccs&lon occur*
ring between July 31 (.S*o. IS) and neccmb.r II. 1*15 (Ko. 38). ... If w«
neglect tho two com'S of July 31 nnd August JO, which commence «t -+0 and +*
respectively, wc have five cases of successive solar ititatlnns In which Uie dlmlnii-
tloi.sof intcnsiry began on the +8 day. This exuct recurrence at the end of
twenty-six days of a marktd diminution of farce pm^cs. It acems !-■ me, thai tha
aeiK'Us ai^ all due to the sun. whuw timo of roLiilon niu>t be nearly twcDty-»ix
•■ An examination wilt show that the nudden rtlmlnntlons of tcrrtstrUl nignctlc
force arc In ncwily every caje ptrctded by a auddi-n Increaae."
In the alwve extract we bave given the author's exact word.i, but,
while thinking with him that those actions are duo to the sun, it
docs not appear to us to follow that the timo of tlio «un'» yt^un
TERRESTRIAL MAGSETISM.]
M E T E O R O L 0 a.Y
177
must be ncarl}- twenty-six days. This a55«mes that the meridian
of peculiar power is fixed on the solar surface. It does not, however,
seem impossible to ima^nc that such a meridian may have a proper
motion of its own. and uideed the planetaiy hypothesis of t)ie origin
of sun-spots would rather lead to this conclusion. But if this be
the case we shall be unable to deduce from recun-ent magnetic dis-
turbances the true value of the period of solar rotation.
87. Repetitions of Magnetic Changes. — J. B. Capello, director of
the Lisbon observatory
{Proc. Roy. Soc, October
1868), has remarked
that at periods of dis-
turbance there are
nearly synchronous
movements of the de-
clination needle during
corresponding hours for
two, three, or more
days. He thus describes
these phenomena: —
"In ipme cases the re-
petition is only in two or
three parallel movements;
in otticrs there are iiue
peiiods of repetition of Boma
hours in duiat Ion. The
repeated peiiods are not
entirclyslinUnr. their piuiaes
being so modified thut in
some cases their Identity can
otily be recojrnlzed by a
very minute investigation.
The same periods, wlien re-
peated, have not ahvays
the same total duration ; nor
do they recommence at the
same precise hour, but
Bometimes earlier and some-
times later, tlie diEferences
varying from a few minutes
to two or three hoars. We
also see that the greatest
number of repetitions be-
long to the night hours,
tliat Is to say, tiiose bout's
when the movements of the
needle are easterly. In the
morning hours there do not
appear to be any well-
m&rked repetitions. There
*re twenty-four examples
now k'ivcn. fliteen of wWch
ehow I'cpetitton on two
days, eight on three days,
and only one where the
carvo appears repeHtt;d fur
lour tlaya. it apiieara that
ill the facts exhibited in
these examples a^ree with
the cosmica] theory; the
vause (existing In the sua
• T Id space) appears to con-
tinue sometimes during two,
three, or several days with-
out undergoing remarkable
traiisfurmjitiiins. The i-e-
petitl<m, being sometimes
cjriier sometimes later,
seems also to indicate that
the cause possesses a proper
the •
Blsts, but only comes again
Into operation when the
earth by its dlui-nul rota-
tion ia placed In a similar
position or conjunction to
that of the preceding days."
Stewart, having com-
pared Capello's curves
with the corresponding
traces of the declina-
tion at Kew, found that
the Lisbon disturb-
ances are almost in-
variably reproduced at
Kew at the same time,
only to a greater ex-
tent, and also that the
same amount of simi-
larity which thevarious
Lisbon curves e.thibit
Pig. 38.
exhibited in the corresponding Kew curves.
The strongest point in favour of the hypothesis is, he thinks, "not
so much the repetition of a single disturbance as the repetition
of a complicated disturbance in most if not all of its sinuosities."
Several examples of this occur in the diagrams. It would seem
that something of the above nattire was suspected by Hi'*nboldt,
the earliest investigator of disturbances. Humboldt was astonished
to discover the frequency with which nocturnal perturbations
oocun*ed, sometimes recurring at the same hour on several successive
in— 9
Table XXIV. — Cates in which tJic EartUs Magnetic Fov'r rf/m/
ished One-thousandth of its Valne or more in 1844-45 t§ 86).
Clmiige
Solar .McrUliiins.
No. of
Dilte
(Jan. 1,
1844=0).
In Huii-
Case.
tliou-
snndtlis.
5 to 10.
1 to 14.
-3t,. +1
nnd otbeis.
1
87 to 81)
-360
+8 to +10
2
iioio nc
-101
+ 11 to +12
3
141 to U3
-107
+ 1110+12
t
189 in 190
-116
+7to+ 8
21;lto2l4
-175
+ 5 to + 6
e
221 to 22!
-135
+13 10+14
7-
267 to 270
-115
+7 to +10
8
273 til 2-4
-104
+13t»i+14
9
292 ro 294
-268
+ Gto+ S
10
323 to 325
-130
+W 10+14
11
3b'l to 364
-165
-3 to 0
12
373 to 375
-210
+9 to +11
13
383 to 3S5
-163
(-6 to -4)
14
416 to 417
-118
Oto+1
15
467 to 4C9
-350
-lto+1
3
.126 to 528
-110
+6 to + 8
17
570 to 671
-164
-2 10 -1
13
677 to 5S0
-102
+6to+ 9
19
COS to 004
-101
■ +5 to + 6
20
606 to 607
-159
+8 to + e
21
632 to 633
— 1.W
+8 to + 9
22
646 to 648
-126
(-4 to -2)
23
65S to 659
-118
+8 to + 9
24
6G8 to 670
-100
(-8 to -6)
25
6.S4 to 687
-100
+ 8 to +10
26
696 t.. 098
-no
(-6 to -4)
27
-O'.tlo 703
-291
-Oto +1
28
710 to 712
-122
+8 to +10
nights (Walker's Magnetism, p. 80). We wDiild make two sug-
gestions before dismissing this subject.
(1) If we imagine that these changes are caused by the solar
influence acting vertically on some susceptible region of tire earth,
then, inasmuch as they occur at the evening or early night houra,
this region must lie considerably to the west.
(2) The region must also have a proper motion of its own (see
Capello's remark). Is it possible that this proper motion is on
the whole from west to east, — a motion which we know is pursued
by meteorological weather, and in which it is imagined (§ 52) that
magnetical weather as defined by us likewise partici}>ates ?
88. Comparison of Declination Changes at Stations near each
other. — Messrs Sidgreaves and Stewart (Pro. Roy. Soc, October 1868)
have compaied together certain cui-ves of the Kew and Stonyhurst
declination magnetographs. These magnetographs are of the feame
pattern, and it was found that on ordinary occasions the declination
traces at both stations were precisely alike. This was confirmed
by placing the curves the one over the other, when they were found
to coincide even in their most minute features. In times of dis-
turbance, however, it was found .that the motions exhibited by the
Stonyhurst curves were greater than those at Kew, and this excess
of Stonyhurst over Kew depended not so much on the absolute
size of the disturbance as on its abruptness.
This feature of the comparison is exhibited in the following
table {XXY.), in which the excess of Stonyhurut over Kew in scale
divisions is compared with the abruptness of the disturbance, this
element being measured by the changes occurring in unit of time: —
Gronp I.
Gi'oup n.
Group m.
Group IV. 1
Excess
(under 6).
Abnipt-
Excess
(under
10).
AbiTjpt-
Excess
(under
20).
Abrupt-
Excess
(above
20).
Abrupt-
2
2
3
0
0
t
1
4
3
8-7
6-4
4 0
3 1
31
2 '9
1-8
3-3
6 '2
6
6
8
5
8
5
7
9
S
4-2
2-6 1
63
3-3
8-7
3-5
• 6--'i
4-7
41
10
10
11
10
10
16
11
13
•6
0
7
0
•8
6-4
4-9
7-4
21
25
25
20
21
21-
22
24
7-3
2-9
10-7
7 0
6-6
ll-.>
9-6
7-8
Means 1-5
3-7
6-6
4-9
11
6-5
22
7-9
It is very desirable that further comparisons of this nature should
be made.
89. Auroral Displays. — ^Theseare veryfrequent if not continuous
near the magnetic poles, while in middle latitudes they are the in-
variable accompaniments of all considerable magnetic storais. Near
the equator they hardly ever occur.
There is a considerable variety in the forms assumed by these
displays, and it is possible that this may denote a corresponding
variety in the cause or causes which give rise to this phenomenon. |J
Loomis (Smithsonian Report for. 1865) specifies five such
vanities: (1) a horizontal light like the moniing aurora or bi'eak
of day; (2) an arch of light vhich frequently extends entirely,
across the heavens from east to west and cuts the magnetic meridian
178
M E,T E O R O L 0 G Y
[teekestrial Mainetjsm.'
nearly at right angles, — in the polar regions five such arches have
been seen at oiicc ; (3) slender luminous beams or columns wcll-
(Icfiued and often of a bright light; (4) the corona, the centre of
which is invariably near the magnetic zenith, but not always
exactly coincident witli it; and (5) waves or flashes of light.
f 90. Auroras exhibit the same annual variation as magnetic dis-
turbances, and arc most frequent about the equinoxes — a fact first
observed by Maizan. Kaemtz in his Meteorology gives the follow-
ing table, which is applicable to European auroras.
Table XXVl.-^Monthl'i/ Frequency of Ei^ropean Auroras.
Jan. Feb. Mar. April. Mny. June. July. Au^. Sept. Oct. Kov. Dec.
1229 307 440 312 184 65 87 217 405 497 285 iliS
Loomis again in the memoir already quoted gives the distribu-
tion of American auroras over the various months derived from one
hundred and thirteen years' observations at New Haven and Boston,
twenty-five years' observations at New York, and two years' obser-
vations in Canada. Hie results are represented in the following
table :-
Table XXVII. — Monthly Frequency of American Auroras,
January...
February..
March
May..]!!.'!!
October
November.
December,.
It appears from this table that American like European auroras
•exhibit a maximum of frequency about the equinoxes.
91. Since auroras and magnetic disturbances go together, it is
natural to imagine that we should have great auroral displays in
year=: of maximum sun-spots. This is found to be the case, and iu
the tbllowing table (XXVIII.) Wolfs proportional numbers denot-
ing sun-spot frequency are compared with the number of auroras
witnessed in Europe and America as compiled by Loomis. It will
be seen from this table that years of maximum auroras coincide
very well with years of maximum sun-spots.
92. "WTiile tno results now given leave little doubC u-s to tlr fact
of a connexion of some sort subsisting between sun-spot^ on the
one handand mag-
netic disturbances
and auroras on the
other, yet it is
desirable to obtain
evidence as to the
closeness of the
connexion between
nd sun-
pots
to
Sun-Spot
Sun-Spot
Auroral
Sun-Spot
Auroral
1750
Number.
~^1
Number.
Nuiiibi.-!-.
Number.
Number.
Number.
31
1794
380
14
18)7
136-9
42
1751
62-1
30
1795
23-8
7
1838
104-1
60
1752
45-9
17
1796
16-6
8
1839
83-4
66
1753
28-9
15
1797
6-5
6
1840
61-8
80
1754
13-5
11
179«
4-6
6
1841
38-6
67
1755
9-3
10
1799
7-1
4
1842
23-0
63
1756
12-2
9
1800
16-6
6
1843
13-1
37
1757
31-9
7
18(11
33-9
6
1844
19-3
39
1768
47-1
1-!
IBdS
64-7
6
1845
S8-3
48
1759
61 -6
16
1803
70-7
6
1846
69-6
64
1760
61-7
23
1K(14
71-4
14
1847
97-4
76
1761
80-2
22
1805
48 '0
14
1848
124-9
72
1762
60-0
19
1806
28-4
13
1849
96-4
69
1763
4S-4
16
1K07
11-1
4
1850
69-8
49
1764
36-7
11
IROR
7-2
2
1861
63-2
65
1765
21-4
8
1R()9
31
1
1852
62-7
67
1766
Ml
6
IHIO
0-0
1
18.-.3
38-5
63
1767
35 '9
9
ISll
1-0
0
18.54
21-0
35
17C8
66-8
30
IKl-i
4-9
1
1855
7-7
20
1769
103-4
40
1R13
12-6
4
1856
6-1
11
1770
9S-5
41
1.S14
16-2
6
18.17
22-9
21
1771
86-6
24
1815
36-2
6
1858
66-2
37
1772
65-7
26
1816
46-9
S
1869
90-3
60
1773
39-7
33
IK17
39-9
7
1860
94-8
48
1774
27-4
33
181N
29-7
11
1861
77-7
36
1776
8 '8
22
IKl'.l
23-5
10
1862
61-0
28
1776
21-7
2-1
1«V(I
16-2
8
1863
45-4
29
1777
92-0
38
18.' 1
6-1
4
1864
46-2
33
1778
161-7
69
1822
3-9
2
1865
31-4
34
1770
123-4
70
i«2a
2-6
1
1666
14-7
31
1780
89-2
■ 07
Wti
81
1
1867
8-8
23
1781
66-5
67
1 Hn
16-2
4
1868
36-8
32
1782
38-7
67
i«'.'«
35-0
12
1869
78-6
1783
22-6
47
l«-.'7
61-2
ir
1870
131-8
1781
10-3
39
IS'.'H
62-1
21
1871
113-8
1785
26-7
66
ISM
67-2
25
1872
99-7
1786
81-2
84
18:lll
67-0
25
1873
671
1787
128-2
108
\m\
50-4
20
1674
43-1
1788
131-3
106
IH32
26-3
13
1876
18-9
lisa
116-9
e«
183S
9 4
11
1876
11-7
irao
90-6
68
1HI14
13-3
12
1877
11-1
1791
46
18.16
69-0
15
1678
3-8
1792
69-9
37
18;«!
119-3
82
1879
7-7
1793
47-3
S3
rA J _j\[\J_
\J
L^
• Of. tf mag
mkh'[
f\iVn
A J
f\N
V
\J '
yv
\) ^
\J ^
that which was
exhibited in § 82.
and which showed
the close connexion
in point of time
between sun-spots
and disturbances.
Loomis has with pj_ gg
this view treated
auroras in precisely the same way in which he treated disturbances
and has obtained the follomug table: —
Table XXIX.— Extent ofSpotUd Solar Surface.
Days before Aurora. Anron. Days after Aaron.
In fig. 39 a graphical representation is given of the likeness
which subsists between tho progfrosa of auroral frequency, spot
frequency, and declination ranges.
UO-3 527 610 61-2 63-1 53-7
54 8 52 5 63-3 61*4 53-8 69i
From which he concludes that "auroral observations in the middle
latitudes of America are generally accompanied by a maximum
disturbance of the sun's surface on the very day of the aurora,"
93. Earth Currents. — These are electrical currents which take
place iu the moist crust of the earth, and were first detected By
W. H. Barlow {Fhil. Trans., 1849). At a later period they were
systematically observed and studied by C. V. Walker {PhiU
Trans. , 1 862). They are now continuously recorded by photography
at the Royal Observatory, Greenwich. Earth currents are particu-
larly strong during magnetic disturbances. Sir George Airy has
graphically compared together certain magnetic disturbances as
recorded by the Greenwich self-recording magnetographs and the
simultineous earth currents recorded by appropriate galvanometers
{Phil. Trans.j 1868), and finds it almost impossible to avoid the con-
clusion that the magnetic distmbances are produced by terrestrial
galvanic currents below the magnets. Tlie likeness betn'een the two
systems of graphical representations is unquestionably very strik*
ing. But, while there is no doubt an intimate connexion between
earth currents and magnetic disturbances, there is one circum-
stance which should make us pause before assigiiing the former
as the complete and efficient cause of the latter. It is thus
indicated by Lloyd :*-
" When we examine the cmTes in wbich Mr Cariow has represented the conrM
of the galvanomerric deflexions caused by thu earth ctirrents, we observe lliat tbo
regularity of that course is continually Intcrrupttd by rujiid reciprocating mora-
ments in which the needle oscHlaics from one side to the other of the icro
altcrnatfly. These movements arc similar to those of the inngnetomctera with
which we are f iimiliir ; but they are much more n-ipld. »»nd bear a Urgcr propor-
tion to the regular changes. ... I have selected for calculation the obser-
vations made during the six hours commcncinic at 3 a.«. <>x May 29. IMS, thnt
being a period of comparative disturbanco. The »um of the «hang:e* of tho
galvanometer needle during that peiiod, on the Derby and Ru(iby line, ««•
equivalent to 671 divisions of the instnmient— tho mean d.iily range for the
entire week being l\A divisions and the ratlo=£0. . . . 'I'he sum of the
changes of tho Greenwich declinometer during tho same period was only M
minutes, the m» nn dally range being 12-4 minutes. In like manner tho sum ol
the changes of the horirontal force was -OIM and the mean .lally ranjro -0034.
The railo Is accordingly the sam-' for the two magnetic elements, i-nd Its amount
Is 4-6. or less than one-tenth of the corresponding ratio in the csm! of the gnlvnno-
metrlcal changes. Wo learn therefore that the rapM cliancts of the caith
currents arc much gicoter In propoitlon to the regular dally changes than lh«
corrcsponcUiig movements of the magnetomclcrs."
We shall rottim to this subject in a subsequent part of this article,
94. Inequalities in Terrestrial MagnHism caused by (he Mo<nu —
Krcil in 1841 was the first to point out that the moon has a small
influence on tho position of the declination needle, and ehortly
afterwards the same fact was indencndently discovered by John
Allan Broun. Tho more recent observations of Subino and of
Broun, but especially those of tho latter, have thrown much light
upon the nature of this action. As tho lunar influence is not
generally large, it is necessary to free the observations from tho
results of other inequalities, and tliis has bt-ondonc by tho two
observers above mentioned. Tho results given in Table XXX.
have been obtained by Sabine (see "Walker's Magnetism).
95. Thus (1) tho mean efl^ect of tho moon upon the declina-
tion needle is to cause in each lunar day a double oscillation, and
Sabine has shown that tlie lunar influence upon tho other magnetic
elements is of a similar type. {'2) Tho turning points for both
hemispheres are in nil cases not far removed from the lunar hourt^
I TVoiu. Rov. Irish Acad., xxlv. ll-V
pSRRBSTKIAL MAONBTISM.] METEQEOLOGY
Table XXX,-ifca,i Lunar-Diumal rarialim in Dtdinatim.
St Releiu
170
latter!" We have iZ:;,^ltkItZ^!^Zt.T''^''' ''''
Febrnury, Jtnrch. April,
May, June, Julv . .
I Aueust, September. October'..
I Movember, December, January
yef^:r.trrj tTj'^\T^\ ^*J" ^^'^'^ -"S- ..c gre..ur ac
.^tioV^the^rte'^n/th^' 'firx^" "-^^ •^"'"''"■' ^"^- rv''^^) -d's{et^/p%r''z"°if rs^f hj'^ "^^rf
^ n..o.t aecMe. at th^ii-.eiil^tr^l'fc-"'A^^^^ I XVLl /ii! ^^ ^J^:^£i^-.^ ^^
Trevanurum. and has ohtaJnori . ^""'*'^*"^3 o* tne lunar influeEce at ,„ -^-^J
studied with much success the t.T f/-"^'-?™"" has recently
Trevandram, and hS obt^inedCm^"'"'' "^ *' '"^a' '">""«»« at
first result was that the naLre„fTJY<.i'"^''£"""' ''^"'*'- His
clination needle at Trevand^m / tne luattr in&ueuce upon the de-
and that the southe™ Iv^„ /? f"*? "P°° "»« «'■"« »f the yeaj-,
drum during So m'^te ?n,l i ""'M"'"'" P^-^dominatos at Treva^l
youths, if t Scf thrLt '^^Tl^'T'l^^^f^
"TJT" •■'■■ '^ '" «' "» «'^ ioj /s ^
anim aunng the winter and f),= n„-.vx*^,.'""ai; irevan- ' -" "^-i 499 499 507 ink VS £j.
declination needle at TreraX,™; *'"?" "^ *■»« °">'"' <»> th.
year during the day thrduHn^ tl,^''^'?."' 'rl'"^ °'°''"' "f 'he
(XXXl.) gfves the Ly and nllft .t;i°l It' '°'-'™"'« ^^'''^
and their ratios:— "'S'"^ 'anges lor the various months
<i|rer£rtf L^|rasfd^^?e::^;7-r '"^ '^^ ^ "
is greater for perigee than for ano^« I "J^"''","''' variation
mean ratio of the apogee effect tofh. \ ?""" ^as found that the
nearly He remark^ tfat ■'the ratio of tK ''^ ■"' *^ a^ 1 to 1 -24
from the earth in the half orhit »l„^. ""P"" * "^an distance
orbit abdut perigee neariy as 1 nr t .T^'" ".*° """' '" "-^ ''alf
l;23 nearly, iJe sfe tha? L mean r ' °« Vf. ' '"''' "'' ^'"^ '^
distances are in the approxim"^ ratio? or°tI "'• ™"''' ^°' «>^ t'^"
ino.n'8 distance from tfie carTh as ; ' !» *i '"^'"^-' '"'''' °^""'
99. Lnnar-Diunial Vari^i'^ ,i ^*/°'7 »f the tides."
Academy of iiencc i"' 8^2 coSe^ t'li^Tth^'^ \ "" '"'P^"^'
Prague and Milan tend to show f J. ■ V "l? observations at
thelunarvariations Sabirterw,.; 7.""^''°"°'^* ^"'a^ Period in
Toronto observations and a so S ' f"'"'- ,^^1,^' 'l^^ '^'■^™«d the
observations with the v"ew of ieeU nf:f ?":> ^«") t^e Hobart Town
come to the conclusion tha? there k^r,„ '"'P"^"' Point, and has
lunar.v.riation correspondin' to t f„ ^ systematic difference in the
diurnal variation, but merelv s, !l. '''>"°"'al Period ofthesol^r-
be reasonably exMcted .!^ ■ i - ^"*' fluctuations as mieht
which they rlpresTnt ■ ~''^'''™g the shortness of the pSs
obsTAatlor,sTith ?h?fi™':?7Hr''"""'°°,-<'^ '^™"''^ Trevandrum
^nbject For this purpTse ^'e^^rvr^fke'n th'^ ""^ "-fl °° '''^
d>umal variations recorded by him for t i '"^"?^' "^ *^ '""ar-
We h»ve in the first place^roZed tW '°™"' '"' "^'^ J'^ar.
threes, representing quartcrly^reS *fe , ranges together into
aether tEeso .ua^rly reslr'yl'aro?^^^ auYforTri'f
He heliev^es^ that'such ai-reTr^hTn,^ n^s'" 'nVSial^tl' 'V''-
lunar.diurnal variation. There are d,n-ir„Vi "*, ^^^^ ''a™ »
to tliis observer, four electrical mt?;™^^^ " • """ ''''^'' according
tive, each nia:rimum betrdi"aXro7tC'''™/"/' *'™ "'^
point of no current. His ?esSts lil-.i! l-^ •''"'' ^^ * ^"^ "^
tion or lagging of the LtWnJ.^7 •'?''"\="•'e'''arreta,da-'
sponding pS of the mion '^ ^f sanations behind the con*
but thesl rVe coSi^^n^Jrotfu^rot-rvl-^ont-^ ""-^
sunteJ^L^^^i.r irrrSyfl^^^^'-S P-^^P^^ *»■«* the
sttT-^V're""" "^ -a."^"- th^at S ^nrli^Tnr
of the'R^dcliffetbt^i-at n; '(^' foTime'toTe "' ^'r?'' ^T-^
in years of maximum sun-sno^ tJ^. ™f " ^^^ conclusion that
occurred under north-eSst wim], » faximum barometric prc^iLro
west, while in veara^f\r;'Ti' ^""^ "■" minimum under south-
minimum pres^urlst^oknW^? sun-spots the maximum and
east winds.^ He came like^se ff Pf '"^lyundcr north and south-
difference in dist^Ztion o^ <^« conclusion that, besides this
the forces whijh rive rise to th?!''"''''" ?'•'•?*' "^^^^ -"arth,
appear to be more^enerStict '^^ '"^'^'"ents of the atmosphere
ininimum sun °pots ^ '° ^"^^ of ma.ximum than in yeis ol
me't^iodtf'oSSn^Ltfo^at"" '■■''" '?,"" *PP<=*^ *» ''^ *he best
weU known ttatd°uin:TumZrTe° ^f "P'""?^''* P"*^'" ^^ '^
have a peculiarly low °andZ '"tenors of large continents
high atmospheric pTessurewhiirr.'"^ "T"' =" P'i'^"''
reverse obtains dLiag the winter monf>,^^n",1° •'='"="y. ">»
Cnd t^o ba „i^„rT"^"' *''"' peculiarities of distribution will U
tho in^i:^"^r™te%tJ^"reri^^Lt bS^!
180'
JIETEOROLOGY
[terrestrial MAONETISM.
Broun, Charles and Frederick Chambere, Eliot, and Hi'.l, and the
followin" conchision is the result of their labours. We may assume
that the Indo- Malayan region has for the mean of this year a
barometric pressure ]irobably below the general average of the
earth. We miglit therefore imafjine that during yeai^ of powerful
solar influence this peculiarity would he increased. Now these
V^servers have found that in this Indo- Malayan region fhe
Urometer is abnormally low during times of maximum sun-
spots. Again, western Siberia is a district which in the winter
season has a pressure decidedly above the average, and we should
therefore imagine that during years of powerful solar influence this
wint,=r pressure should bo peculiarly high. But this is what
Blanfora has found in his discussion of the Russian stations to
correspond with years of maximum suu-spota.*
Again, Frederick Ch.imbers has enunciated the following laws as
resulting from his discussion of various meteorological records:—
(1) Variations of the sun-spot area are succeeded some months
afterwards in the Indo-Malayan region by corresponding abnormal
barometric variations, a high barometer corresponding to a mini-
mum of sun-spots.^
(2) This lagging behind is greater for easterly than for westerly
stations. In other words, this, like other meteorological phenomena,
appears to travel from west to east.
We may tlierefore coni'ludo that the barometric evidence a^far as
it goes is in favour of the hypothesis that the sun is most powerful
at times of maximum sun-spots.
105. Rainfall— Hriqhts of Rivera and Lakes.— In 1872 Mel-
drum of the Mauritius Observatory brought forward evidence
showing that the rainfalls at Mauritius, Adelaide, and Brisbane
were on the whole greater in years of maximum than in years
of minimum sun-spots. Shortly afterwards it was shown by
Lockyer {Nature, December 12, 1872) that the same law was
observable in the rainfalls at the Cape of Good Hope and Madras.
Meldnim has since found that the law holds for a great num-
ber of stations, including eighteen out of twenty-two European
observatories, with an average of thirty years' obseiTations for each.
The results are exhibited in the following table (XXXIV.) :—
Name of Observatory.
, St Petersburg..
. Chilstiania ....
. Edliiburch
. VlennR
. Nlcolaleff..
-fl3-08
-H9-6S
-f(i6-85
-22-79
-HO'95
+ 0-44
+ 22 02
-HI T3
-H9-90
-H 8-90
-(-1384
+ 9-94
— 18-35
+ G-44
- 6-16
-11-81
-H8-30
+ 4-06
It would, however, appear from the observations of Governor
Rawson that the rainfall in Barbados forms an exception to this
rule, being grcnttst about the times of minimum sun-spijts.
106. Gustav Wex in 1873' showed that the recorded depth of
water in the rivei-s Elbe, Rhine, Oder, Danube, and VistulaJor the
Bix sun-spot periods from 1800 to 1867 was greater at times of
maximum than at times of minimum sun-spot freniicncy. These
conclusions have since been confirmed by Professor Fritz.*
Quito recently Stewart (Proc. Lit. and Phil. Soe. of Manchester,
1882) has treated the evidence given by Fritz as regards the Elbe
and Seine in the following manner. He divides each sun period,
without regard to its exact lenL'th, into twelve portions, and puts
to'^ether the recorded river heights corresponding in time to
similar portions of consecutive sun periods. He finds by this
means residual differences from the average representing the same
law whether we take the whole or either half of all the recorded
observations, and whether we take the Elbe or the Seine. The
law is that there is a maximum of river height about the time of
maximum sun-spots and another subsidiary maximum about the
time of minimum sun-spots. There is some reason too to think
that the Nile ami Thames agree with those rivers in exhibiting a
maximum about the time of maximum sun-spots and a subsidiary
ma.ximum about the time of minimum sun-spot-s, only their aub-
wdiarv maximum is greater than it'ia for the Elbe and Seine.
I Natvrf, November 2.*S and December 2, 1880.
'Kalurt. Mnreh 18, 18S0,
• Jjimnfrur ZeilKHiifl. IB73. „-.,.> j
'tt/rbrr dir II li-hmiim dor SotinmJiKkm Periodi lu dm ^afnttitOnn ma
.f V ■rt-.n'rt", rft, „ ^«**<Af/Miinjm rf^r £r(/«. Haarlem, 1878.
107. In 1S74 G. M. Dawson came to the conclusion that the
levels of tho gicat American lakes were highest about times of
maximum sun-spotji. In this investigation the value of the
evidence derived froni rivers and lakes is no doubt gi'cater than
that derived from any single rainfall station, inasmuch as in the
former case the rainfall of a largo district is inte^-ated and irregu-
larities due to local influence thus greatly avoided.
108. Dr Hunter, director-general of statistics in India, has recently
shown (A^//ic(ecii/'iC«i<iir!;,Movember 1877) that the recorded (amines
have been most frequent at Madras about the years of niinimuni
sun-spots — years likewise associated with a diminished rainfall.
109. Winds and .«oriM.— Meldrum of the -Mauritius Obser-
vatory found in 1872, as the result of about thirty years' observa-
tions, that there are more cyclones in the Indian Ocean during
years of maximum than during yeai-s of minimum sun-spots.^ The
connexion between the two is exhibited in the following table ; —
Table XXXV.— CoiiiTJitri'soit of t!te Yearly Number of Ci/drnta
occurring in llu Indian Ocean mitli the Yearly Number o)
Spots on the Sun.
rega.d&
Sun-
Number
ot Hlirrl-
Noraber
of Storms.
Number
of Wliole
GalM.
Number
of Stiong
Oalet.
Total
N'uniberof
Cyclones.
of
Cjcloncs
In Max.
Spo.8.
rcrtods.
(
1S47
5
0
0
0
■■•>
Max.]
164S
1849
1850
1R51
lSi2
1(1.13
1854
«
3
4
4
t
1
3
2
0
3
1
1
3
6
0
0
2
0
0
1
0
1^1
7
8
*)
MIn. J
16.15
lejd
1857
1818
1859
3
1
3
3
3
0
2
1
3
6
0
1
0
2
4
if
4
15)
Max. -i
1850
7
2
0
(
1861
6
2
2
11>
1862
4
2
2
1863
S
I
1
1864
2
1
0
(
1865
2
3
0
-)
Mln.J
1866
1
2
1
4
■\
1867
0
2
6)
186S
3
2
0
1
3
3
'1
Max. -
ls;o
1971
1 1872
1
3
6
3
1
3
3
1
llj
13
1873-| *
3
0
12
-UjitoUB)' 31.
In 1873 M. Poey* found a similar connexion betireen tbe hurri-
canes of the We3t Indies and the years ot maximum sun-spots.
He enumerated three hundred and tifty-seven hurricanes between
1750 and 1S73, and stated that out of twelve maxima ten Agreed.
110. In 1877 Mr Henry Jeula, of Lloyd's, and Dr Hunter found
that the casualties on the registered vessels of the Urvited Kingdom
were t7i per cent, greater during the two yeai-s about maximuiii
than during the two years about minimum in tbe solar cycle.
111. Temperature. — Baxendell, in a memoir already quoted, was
the Jii-st to conclude that the distribution of temperature under
different winds, like that of barometric pressure, is sensibly in-
fluenced by tbe changes which take place in solar activity. In
1870 Piazzi Smyth published the results of an important seriits
of observations made from 1837 to 1869 with theniiometera sunk
in the rock at the Royal ObserViitory, Edinburgh. " He con-
cluded from these that a hent wave occui-s about every eleven yeai^s,
its maximum being not fur from the minimum of the sun-spot cycle.
Sir G. B. Airy lias obtained similar results from the Greenwich ob-
servations. In 1871 E. J. Stono examined the temperature obser-
vations recorded during thirty yeara at the Cape of Good Hope,
and came to the conclusion that the same cause which leads to an
excess of mean annual temperature at the Cape leads equally to a
dissipation of sun-spots. Dr W. Kbppen in 1873 discussed at great
length the connexion between sunspoLsand terrestrial temperatur«»
and found that in the tropica the maximum temperature occurs
fully a ypar before the minimum of sun-spots, while in tho son«9
beyond the troi>ics it occurs two years after the minimum. The
regularity and magnitude of tho temperature wave art most strongly
marked in tho tropics.
112. The evidence now given appears at first sight to be antago-
nistic to that derived from tlie otner elements both of magnetism
and meteorology, and to lead us to conclude that tho sun heats us
most when tlicre are fewest spots on its surface. This roncliuioo
will not, however, bo strengthened if wo examine the subject with.
greater minuteness.
B Br. Atfoc. RfTorlt, 1872.
A A. Polly, Sur let Rafporti entttUt Tartift SoIa{r«$ *l ta Ouroffant detAntOlti.
lU rAtlantique-Aard, tt dtf fOcean /ndUn Sud,
iurnace itself wa;'Vo=:;;s^ic;^,o;t'i„7T; ^'^-^-^^-^^i^e I j;:::::' ir^g:^^!; i^i^^^ l^jf ^"" t^^ir^ft,^:;^::;;:-
a low mean temperature occurs when tLrT;l\ sta ions system observed around tl.e sun'sl ml, n„ 'n J "'? ™nvcction
rainfall and a giat amount of ooml. I . u • ''""^■■'"y large us in this sunpQsitiou And if tL .„ »■ ^ oc.as.ous confirm
l'!rL°i.',!'Ar:^'"-.«f ?"n-P0ts than by tl.Tof I o(l\ZT^l:^.l°"J."^}'''^.' conclu1_io„s^b'y direct observarto,,,
determinations liav«
trial te-ip' ratur" From This -tJ^ ""'"1^^ "'^^ ^''"^'' t"^=-
sun-spots is followed in ? d,v J fP'^^"' that a rapid increase of
temperature ranrat Toronto^ Nn? ^^- '" "'"T,° "^ ^''^ '''""•■'l
ture'range ^ost^^robabh denotes ^,^1:^^;^ ''"''"'' '^-"i'"^- I '""Sy is then pecul
Y<^ are thus led to associlte an fncrea e of ,M° ^'^'' '".t'^^', ""'^ °^ ""' latter fact
thc"nttetXgl?ftttntrn?UtS"o'f° thl ra^y'"'^'"<'l '^^'
T..ost active at times of niaximC sTu srots and ttfJl''™''"'"'^
oiogy is not ^rsv1^nfa\ t;;f f?:;ti::tt[r ■"^'^°'-
this basis to mtoind t'e t«o fol^owf^'^f''''';""'* P™ceed from
place, what is t° o "t e of the »i^ - ^ "" °' '"'" "" ^"^
loagnetism? and. secondly why^sth^s infl nJi"'"'' "'"!" "^"^■''""'
perceived thin ,.»,.t-„^, r ■* ' ^^"y '^ *''=» influence so much more easily
• ■ ' __ ..e^'^ ,"'.'"> "^o""'- supposed that tho
of the sun upon' tie earth ' We havlr^jy^'Tf^^Snetic action
reasons,-firs , because fom whn, , "^"""l^^ '''"" this for two
appears to us unlikelv that .t ^tnj" "°" ^'"'"' "^ ^^^ '*'"' it
yature upon the eartCsfnce'^b'ody Vrh^h t^nirle^r" "' ""^
ing ve,y strong m,<j„etic T,ro,ZtJ.uTJ.V'JP."^}"'' P"^"^"
n °t°''^*° P""'"" '"'"• ^" ™"'J have the°rmo!elec c cu ion L
ing ve,/ st^ng magnetic nro,^,-*' a h.gh temperature possess- ever ; L s4onJ deahwiTh ",? ""'■'°"' *" '^' atmosphere «d,at-
when we are caUed .^^n , ^^ "■ *° °' "^^^ ""e time has yet arrived tlie dai v m,Vn»H ■ .• "^ evidence that changes in the range of
discove^oTf^rthertr'irth ""°^ ^^"''''"' "^oessary a^ids to the i^VoluLTZT ToTZCf^/1l' ^°"''^^^^^^^
mparatively large amaoat of spotted area i ft-,, » , ,^ .
18a
METEOROLOGY
[terrestrial magnexism.
*19. Let ns therefore dismiss the hypothesis of direct action and
oonsiJer that of Faniday. Wo know both from observations of the
declination and horizontal force {Proc. Jioy. Soc., March 22, 1877,
aaJ Phil. Trans., 18S0, p. 541) that the action of the sun in pro-
ducinj; diurnal variations of these elements is one and a half times
'•s powei-fnl at epochs of maximum as it is at epochs of minimum
sin-spot frequency. It is hardly credible that there should be
such a great ditference on these occasions in the sun's heating effect
upon the great bulk of the atmosphere. . Meteorologists have never
©bserved such a difference, nor is there any marked corresponding
inequality of diurmd temperature range. Meteorological evidence
ie thus against the diurnal magnetic changes being due to the
heating up by the sun of the great mass of oxygen which constitutes
llie magnetic portion of the earth's atmosphere. Again, as there is
ft preponderance of hot oxygen in the northern hemisphere during
the June and in the southern hemisphere during the December
solstice, there ought according to this theory to be a. well-marked
annual variation of the magnetism of the earth, the northern hemi-
sphere being at the same time differently affected from the southern.
But there are no traces of such a phenomenon, the annual and semi-
annual variations which we have alreudy described (§g 64-67} being
of quite a ilitterent nature, and none of tliem very large.
120. Precisely the same objections apply with even greater force
to the fourth hypothesis. It seems impossible to allow that any
heating effect of the crust of the earth caused by the sun can be one
and a half times as great at epochs of maximum as it is at epochs
rf minimum sun-spot frequency.
121. We are thus driven by the method of exhaustions to look
lo tlie upper regions of the earth's atmosphere as tlie most probable
seat of the solar influence in producing diurnal magnetic changes,
and it need hardly be said that the only conceivable magnetic cause
•opable of operating in such regions nnist be an electric current.
Now we know from our study of the jiurora that there are such
rurrents in these regions — continuous near the pole and occasional
in lower latitudes. A good deal has been said about the difficulty
of imagining a daily set of currents to be generated in regions of
Buch imperfect conductivity, but we shall see by and by {§ 134)
♦feat there seems ground for imagining that their conductivity may
ke much greater than has hitherto been supposed.
122. Analogies hcticccn the Meteorological and Magiidical Si/sk^ns
e^ the Eiirih. — We liavi? in the first place a zone erf maximum ter-
restrial temperature, the middle line of which is nearly coinculent
not only with the geographical but likewise with the magnetical
•quntor. Again, there are possibly in tlie.norllicrn hemisphere
»i\o poles of gieatcbt cold, which possibly do not greatly diticr in
position from those sjiots which wc have called magnetic poles or
fpci. Abuut the soutJiern hemisphere wc have no information.
Furthermore we believe that the hot air is carneil from the zone
•f greatest heat to tlie place or places of greatest cold by means, no
*oubt, of the return trades wliicli blow in the upper atmospheric
regions. The hot air divides at this zone, one part blowing north-
wards in the nortliern and anotluT soutliwanis in the sonlliern
keinisphere. Now this zone, from which tlic anti-tradts divide,
\i*a an finnual motion of its own, being found farthest noith at the
June solstice and farthest south at that of December Probably too
the northern system is strongest in June and the southern system
HI December. If we now turn to the solar diurnal variation of
Magnetic declination, wc find here also a northern and a southern
system (§ 41), the type of the one being antagonistic to that of the
other. Wc find also that the northern system is strongest in June
and the southern system in December.
Again, it seems probable from what wc have now said that the
anti-trades, strictly speaking, have reference not to the geographical
equator and poles hut to the zone of maximum and the poles of
■oinimum tempiratuie. Now, turning once more to the diurnal
•ocJUations of the iU-clinatiou needle, it .scenis probable that the
directions ea^t and west must be interpn ted as having a reference
not to the geographical but to the magnetical pole (§ 45).
These analogies must be taken for wliat they arc worth. Our
•hjcct in introducing them lias reference to the ])revious discussion,
from which wc concluded tliat the magnetic inliucncc of the sun is
probably due to cunvnts in the upper rc-jlon of the atmosphere —
the cause of whicli we were content to leave in abeyance. Now
these analogies would had us to suggest that this cause, whatever
it is, may perhaps be found to be ivlatcd to tlie convection sy;item
nf the earth on the one hand and to the magnetic .system .on tho
•thcr.
123. Amiloijics Irltrccn Mdcorologirnl nml Magnrfiral Wvathrr. —
These remarks arc borne out by thu further analogv whieh apj'cars
to subsist betwixt what wc have termed nut.orulngirnl and inng-
netical weather. Let us take the Kolnr-iliurnnl variation oi dedina*
lion. Not only is tliis variation similar in form to the dinrnal
variation of atmospheric temperature (g 37), but the i-anges of tho
two have a similar annual variation. And, as the element of
meteorological weather aficets the orderly march of tho temperature
range, jubt so tho clement of magnetical weather aif-icts the orderly
vmrch of the declination range.
Furthermore, just as tcmperatnre-range weather progresses from
west to east (§ 52), so declination-range weather would seem to pro-
gress in the same direction as the other (§ 52) although at a greater
rate. It will doubtless require a more extended investigation to
mike «3 quite sure of this latter point ; neverthelesfl we do not
perceive the valiility of the objection that is sometimes made to the
hypothesis of progress in magnetic weather on the ground that
magnetic influences are known to affect all portions ol the globe
simultaneously. It will, wc think, bo perceived that in the above
statement no supposition whatever is made with respect to the rate
of propagation of a magnetic influence through the earth; this may
be instantaneous or it may not. It is supposed that wo have here
a travelling cause of excitement, say a travelling cause of currents
in the upper regions of the atmosphere which progiesses from west to
east and alw^ays produces its most marked effect above those regions
where it passes^ust as the sun itself in passing from east to west
produces a magnetic effect tho various phases of which travel from
east to west with the sun which causes them. We think too that this
hypothesis of travelling causes of magnetic change is strengthened
by the facts observed by Capello and described in § 97.
124. If, however, the objection made to this hypothesis refers to
the fact disclosed by Broun (§ 85) that changes of horizontal force
appear to take place simultaneously at distant parts of tho earth's
surface, then we think that analogy should lead us not to deny the
possibility of a travelling magnetic excitement, but ratlier to suggest
the possiijility of there being some meteorological influence which,
like the magnetical one above mentioned, may be found to take
place simultaneously at different part3 of the earth's surface. Now
Broun {/'roc. liotj. Soc, May 11, 1876) has given us preliminary
evidence for supposing that there are simultaneous barometric varia-
tions. For instance, there was a barometric maxiniunx at Hobart
Town, Piking, the Cape, St Helen.i, Makerstoun, Singapore,
Madras, Simla, Ekaterinburg, and Bogoslovsk about the end of
Marcher tirst day of April 1845. There appears to have been a
simultaneous increase of the horizontal force of tlie earth at various
stations much about tlie same time, and there also appears to have
been a short-period maximum of spots on the solar surface. BrouD
has likewise registered simultaneous barometric varintions at Slnga-
pore. Madias, and Simla, for the first tliree months of 1845. From
these it would seem that simultaneous barometric maxima are
possibly coincident «ith rapidly increasing sun-spot areas.
Again is it not absolutely certain that if there is a sudden increase
of solar power this must mean an iuerease of heat communicated
to the earth, although it may be diflicult or even impossible to
obtain expi-rimcntal eviilcnce of such a fact? All these arc sub-
jects whieh require further investigation.
125. Further Pcmarks o7i the Solar-Diunial Variation oj
Declination. — \w. % 24 we have asked how far the action of the solar-
diurnal force upon a frcely-snspcnded magnet is due to currents
acting directly upon the m.ignet and how far to a change produced
in the magnetism of tho earth. Some light appears to be thrown
on this point by the behaviour of the needle at places near the
magnetic pole where the dipping needle is nearly vertical. On
opposite sides of this locality the declination needle jioints in op|K>-
site directions. Now su|»itosc that wc have a set of such needles
placed all round this region. It seems a legitimate generalization
trom tho oUervations described by Sabine (§ 4j) to conclude that
if wc place ourselves above the centre of any of these needles at
8 A.M., and look towards its market! pole, we shall find it in every
case deflected towards the ri"ht, while if we look towards tho snnio
pole at 2 r.M. wc shall timt it denectcd to the left. Now if wo
iinaginc that at 3 a.m. thei-o arc above these m.i^nets (in tlio upper
atmospheric regions) clcctrieal currents of v.hi.h ihc iiorizontul
components form a set of positive currents flowing from the polo on
all sides, then by the known laws of such cnri-eiita the marked jwlo
of all Iheso needles will be dcfleeted townnis the light. Anil if at
2 !'.M. the resolved portions of such currenis should be flowing
towai-ds the pole, then the markcil poles of all these needled will be
deflected towards the left. It thus npiH-nrs (hat this peculiar
magnetic beliaviotir might easily be e.vpl.iincd by a hy|K)thclical
distribution of currents. And In fart in Muh regions we have in-
dubitable cvi.Iencc of tho e.\istemc of currents in tlic upper regions
of the atmosphere. On the oth.r hand this behaviour conhl not
easily be explained by tho hypothesis of M>mc definite temporary
ma«'netic system set up by the .solar Innncuce in the cnrlh, for in
such a case'wo should iaj.igine tliat similar ].oIes of nil tho needles
ought to be deflected towards tho polo of this temporary system,
which is not the case.
126. Another point for consideration is the possible romplexily
of tho solartlinriml variation. For wo. may imagine d) that tho
sun ftcti in mh h a manner as to produce a dinnial variation ; (2) it
may also act like tli» moon (§ 94) and prclucc a scmidiur'nal varia-
tion ; (3) these possible actions m:ty bo accompanied by induced
currents in the upper regions of the ntniosplun: and in iho trust of
the earth ; (4) it is po<MbIc that the sun's rays moy nffecl these
variations or some of them in the way in which Uroun found that
the lunar variation at Trevandrum was olTcctcd by the s.in. It
TEBRESTRIAIi MAGNETISM.]
was found by him tlmt the lunar action was oonslderably In-
-•rc'ased when the sun was above the horizon of the place.
127. We have pointed out (§ 119) that7 while there is a marked
likeness in many resjiects between the diurnal variation of declina-
tion and that of atmospheric teu'pcrature, vc have yet no long-
period fluctuation of the diurnal rauge of teniiitrature at all com-
parable in magiiitnJe to the magnetic fluctuations. It does not,
nowever, seem difficult to account for this difftroncc if we imagine
that the magnetic fluctuations take their origin in the upper atmo-
spheric regions, while the temperature fluctuations are due to the
lower regions of the earth's atmosphere. For, as the sun increases
in power from times of minimum to times of m.iximum sun-spot
frequency, we may iinarine that a continuously increasing amount
of aqueous vapour will be taken into the earth's atmosphere.
Now the experiments of Tyndall and othei-s induce us to tliink
that the air would under such circumstances become more and more
opaque for certain r:;y3 of the sun, and thus a continuously decreas-
ing proportion of the sun's heat would be able to penetrate into
the lower atmospheric regions. This latter influence would triere-
foie operate to cloak, perhaps to a considerable extent, the eflect of
the sun's increasing power ; and this may very will be the reason
why the temperature range at the earth's surface does not exhibit
the same eleven-yearly inequality as the declination range.
128. There seems, however, reason to believe that if we go from
loug to short period inequalities there is a much greater simQarity
in the range of the magnetical' and the meteorological changes
(§113). The explanation seems to be that in the short-period changes
the sun has not time to alter sensibly the constitution of the atmo-
enherc, and hence the proportional increaw of efl'ect experienced in
the upper atmospheric regions is more nearly the same as that
experienced near the surface of the earth.
1'29. MagiKtU DisturbaTuxs.—theK is strong evidence that the
most important disturbances break out very nearly simultaneously
at widely difierent parts of the earth, and that they even aHect both
hemispheres at the same time. Very little, however, is known
about the modm operandi o{ the forces concerned in producing such
disturbances. For instance, it is not known whether a distmbanco
permanoutly afi'ects the magnetic state of the earth, e.g., whether
one of the maguotio elements before a disturbance begins is sensibly
different m value from what it is after the disturbance has ceased
to exist On the other hand we know (1) that disturbances break
out on the very day when there are rapid changes taking pFace
on the sun's surface (§ 83) ; (2) that they generally begin' by
momentarUy increasing the horiz.'ntal force, but that the type
?[uicldy changes, so that during most disturbances the horizontal
orco is diminished (§ 86) ; (3) that large disturbances take place
more i>articularly about the equiuoxes, when, we have reason to
bcheve, the horizontal force of the earth is at a minimum (§ 77).
May we not possibly conclude from these habits of action that at
tunes of disturbance the earth is magnetically in a delicate state of
equilibrium, perhaps having more magnetism than its surroundings
would stnctly warrant, and being therefore inclined to part with
some, and that a sudden increase of solar activity, tending, as sui-h
changes probably do, at first to exalt the magnetism of the earth,
nevertheless destroys its magnetic balance and gives it ultimately
the opportunity of parting with some of its magnetism ? This can
"l^k* '"oi"'l'2'I as a sneculation, inasmuch as we do not know
whether or not a disturbance produces any permanent influence
upon the magnetism of the earth.
130. Auroras and Earlh Currents.— There is no doubt that these
phenomena denote electric currents in the upper regions of the
atmosphere and in the moist conducting crust of the earth The
joint in dispute is with respect to the origin of such currents
Sbuie are inclined to regard auroras as peculiar manifestations of
atmospherical electricity in high htitudes, while others imagine that
such displays are rather of the natui-e of induced currents generated
by small but abrupt changes taking place in the magnetism of the
earth. The advocates of the first view do not deny that currents
taking place somehowin the upper atmospheric regionswill havetheir
conditions modified, to some extent at least, by the inducing influence
of magiictio changes. Nor will the advocates of the inducFion hypo-
thesis bo disposed to deny the possibility or even the certainty that
displays due to atmospherical electricity and not dissimilar to some
kind of auBora take place in some region of the atmosphere. But the
hrst party regard auroras rather as the cause than as the efl'ect of mag-
netic cuauges, whereas the advocates of iuduction regard such displays
rather as tlie efl'ect than as the cause of changes somehow produced
in the magnetism of the earth. And here it is desirable to remark
that the advocates of the induction hypothesis take for granted the
magnetism of the earth and the changes thereof as phenomena for
which they do not profess to account, whereas unless we go to some
absolutely unknown cause (and this is against our present pro-
gramme) we must look to atmospherical electricitv as likely to throw;
hght upon the origin of terrestrial magnetism. "We cannot therefore
dispena with regarding atmospherical electricity as an agent which
may have played an important part in the development of the
jgi^eut magnetical condition of the earth, but we are yet of opinion
M JE T E O li O L 0 G T
183
that, under the present state of things, the theory wh'ich holds by
atmospheric electricity must largely be supplemented by the induc-
tion hypothesis if It IS to explain the peculiarities in type or fonn
of the phenomena which observation brings before us.
131. Professor Tait in his essay OH-thundei^torms attributes ou«
kind of aurora to atmospherical electricity. Such au aurora is, he
believes, the manifestation of almost continuous discharges, liko
those given by a Holtz machine in a vacuum tube. The cn'use i«
condensation of vapour going on very slowly in very large spaces of
air. The electricity is due to previous contact of' particles of ai'
and vapour. The result is that the air-panicles in the mixture in
time acquire a definite difference of potential from those of vaiwur -^
so that, when the latter aggregate, a misty region well cliarged is the
result, and this discharges to the oppositely electrified air a\l round;
132. Again, Professor Stokes, without attempting to account for
the origin of atmospherical electricity, has produced an hypothesis
with the view of explaining the intimate connexion s'ubsistin"
between auroral displays, earth currents, and magnetic changes on
the one hand and outburats of sun-spot activity on the other. His'
idea is that two somewhat distant atmospheric regions A and B are
charged, let us say, with i positive and negative electricity respeo-'
tively ; A induces in the ground below it a charge of negative, B a
charge of positive electricity. At first things are held in this state :'
A cannot discharge either through the upper atmospheric regious'
to B or through the lower regious to the ground beneath it, whilo'
B is in a position precisely similar. Presently, however, an increase'
of the radiative power of the sun is produced. Such an increase
would probably imply not merely an increase in general radiation'
but a particular increase in such actinic rays as are absorbed in the'
upper regions of the earth's atmosphere. 'The layer of atmosphere!
between A aud B will therefore greedily absorb such rays, its tem-j
perature will lise, and, as is known to be the case for gases, the
electrical conductivity of the stratum will be increased. A dis-
charge will therefore ultimately take place in the upper regions'
between A and B ; this will relieve the charges of uegative and
positive in the ground immediately beneath A and B, and these
charges wiU therefore rush together through the ground, producing
an earth current. This eaith current will be in the opposite diiec-!
tion from the atmos|iheric current, and the two will combine to
represent, virtually at least, if not absolutely, a closed circuit. This
ft-ill of coui-se alTect the earth's magnetism and produce a disturbance.^
183. This hypothesis certainly afl'ords a good explanation of the
promptness with which disturbances follow increased solar activitjj
(§ 83). Unless we are to resort to some unknown cause it is diffi^
cult to think of any other possible explanation of this fact. SucW
an explanation appears too to receive corroboration from the fact'
{§ 97) that the lunar influence on the earth's magnetism as observed]
at Trevandrum is greater during the day than during the night, -J
greater possibly too at times of maximum than at times of niinimun?
sun-spots. AVe are therefore disposed to accept this explanation of
the way in which increased solar activity produces magnetic dis-
turbance as the best that baa been brought forward.
134. This does not, however, decide the disputed point how far
these elevated currents are due to atmospherical electricity and how
far to induction. The argument against tlie possibility of induced
currents in these regions is derived from experiments with vacuum'
tubes, aich as those recorded by Messrs De la Rue and Miiller, whichi
would seem to indicate that enormous difl'erences of potential would
be required to produce electrical currents in elevated regions, where'
the atmosphere is very rare. 1
Indeed, on account of these experiments, the measurements of
the old observers, who sometimes assigned a height of more than'
100 miles to the aurora, have been called in question, and it has'
been supposed against direct observation that these phenomena must'
always occur in regions much less elevated. It would appear tool
that such reasons were influential in determining Professor Stokes
to regard the aurora as produced by atmospherical electricity which,)
.as we know from ordinary lightning, presents us with enoimoua
difl'cronces of potential ; but it is to De remarked that lie has care-
fully guarded himself against the possibility of laboratory experi-
ments with vacuum tubes not being strictly analogous to that wliich
takes place in the upper atmospheric regions. Now it would appear'
that recent experiments by Hiftorf throw some doubt upon the'
strictness of this analogy. The highilifference of potential required
to force the curreut through vacuum tubes is, according to this
observer, due in great part if not entirely to the passage of the fluid
from the terminal to the residual air of the tube, so that the poten-'
tial requisite to pass a current through a tube of double lergth is
not sensibly greater than that required for a tube of single lengthj
The whole subject is one which demands further investigation:
naeanwhile we are not disposed to assert the impossibility of induC]
tion currents taking place in the upper atmospheric regions. . "
135. Let us now consider whether the form or type of the eartS
currents observed during disturbances favours the presence of induc-
tion to any sensible extent The remarks of Dr Lloyd already
quoted (g 93), which are confinned by the Greenwich ob8erva'.l..:-3,
seem to be decisive in this res^jectijhese may be intei^ueted in
18+
METEOROLOGY
[TEKKESTniAL MAOKETISM.
ttie tollowingniaimor. In a magnetic disturbance we have fre-
rjuentiy a general displacement of the various elements — thehori-
juontal force, for instance ; now on the curve which represents this
slow but considerable displacement a large number of comparatively
small but very abrupt changes are superimposed. These latter
appearances are invariably accompanied oy quick and strong alter-
uations from' positive to negative of tho earth currents, while the
former slow motion, although it- may be of large range, hardly
appears to have any galvanic equivalent at all This would appear
to favour the induction hypothesis, according to which small but
iabrupt magnetic changes should givo rise to strong earth currents
alternately positive and negative without reference to the position
of the magnet above or below its normal at the time.
136. Another fact bearing upon this hypothesis is that mentioned
in § 88. From this it would appear that on ordinary occasions the
curves recording the progress of the declination needle at Kew and
Stonyhurst are as nearly as possible identical, but on occasions of
ilisturbance the range at Stonyhurst is greater than that at Kew by
an amount not apparently depending so much on the magnitude of
the disturbance as on its abruptness. The introduction of the
element 'of abruptness would appear to be in favour of tho mix-
ing up to some extent of induced currents with the phenomena in
question.
137. Sir George Airy has not been able to detect any resemblance
in form between the regular diurnal progress of the magnet and that
of the earth currents. It seems, however, possible that the peaks
and hollows alluded to in § 73 may form an important and integral
part of the daily magnetic movement, and there even appears to be
some evidence that the diurnal progress of the earth currents bears
a nearer resemblance to that of the peaks and hollows than it does
to the progress of the smoother curve which is usually held to
represent the diurnal variation. But this is a question which can
only be decided by more prolonged investigations.
138. To conclude, there can be no doubt that at times of great
magnetic disturbance we have currents in the upper atmospheric
regions and in the crust. of the earth which, so far as we can see,
must either be due to atmospherical electricity or to induction, or
to a mixture of both. Tho proportions of this mixture can only be
decided by further inquiry and by the multiplication of stations
where atmospherical electricity and earth currents maybe observed.
It ought to be mentioned that the experience of the Kew observers,
as far as tlus extends, seems unfavourable to the hypothesis of a
connexion between auroras and atmospheric electricity.
139. Lunar- Semidiurnal Variation. — From the fact observed by
[Broun (§ 98) that the moon's mngnttic influence is as nearly as
possible inversely proportional to the cube of the moon's distance
irom the earth, it is impossible to refrain from associating it either
'directly or indirectly with something having the type of tidal action,
but in what way this influence operates we cannot tell. Is it
possible that the earth currents observed by A. Adams (§ 101) are
induction currents generated in the conducting crust of the earth
by the magnetic change caused by the moon, — inasmuch as these
cuiTcnts were found by him to bo .strongest in one direction about
the lunar hours 3 and 15, when the;unar-diurnal magnetic effect
is changing most rapidly in one direction (§95), while they were
Tound to be strongest in an opposite direction about the lunar hours
9 and 21, when tho lunar-diurnal magnetic effect is changijig most
rapiiJIy in an opposite direction ?
14{X We might perhaps, expect from the analogy of the titles that
the sun should possess a semidiurnal magnetic effect similar in typo
to that of the moon. Now Sir George Airy in his analysis of the
earth currents observed at Greenwich {Phil. Trans., 1870) during
days of tranquil magnetism has detected in such currents a semi-
diurnal inequality having maxima in one direction at solar hours
Sand 15, while it has maxima in tho opposite direction at solar hours
9 and 21. . The reference to solar hours in this inequality is thus
precisely similar to that which the inequality observed by Adams
Dears to lunar hours.
141. If there are induced currents of this nature in the crust of
the earth, we might naturally su|>pose that there will be correspond-
ing currents iu the upper regions of the earth's atmosphere, and in
accordance with the suggestion mado by Professor Stokes (§ 132)
we miglit perhaps suppose that these currents will be strongest when
the uppor atmospheric regions are heated by tho sun and thereby
rendered better conductors. Is it not possible to suppose that the
influence of dayliglit upon the lunar magnetic effect discovered by
Ilrouii (§ 97) may be due to this causi*, and may it not also induce
us to recognize thcjpossibility of a maximum lunar influence (§ 99)
ut times of maximum sun-spots, when there is reason to believe that
bolar radiation is most powerful ?
142. Secular Variation. — Sabine and Walker are agreed in
5"ogarding tliia variation as cosniical in its origin, and they aro
apparently of opinion that it is caused by somo change in the con-
dition of tho sun. It seems difficult if not impossible to attribute
it to anything else, since the terella of Hailey cannot be now
regarded as having a physical existence. Again it is more than
possible — it is p_robubiy — that there wo solar variations of much
longer period than eleven yrars. On tho other hand the evidence
given in § 81, tending to show that an access of sun-spots producesa
change in the magnetic state of the earth consistent with the hypo-
thesis that the magnetizing power of the sun has then been
augmented, requires to be confirmed by more observations ; aud
even then it is certain that this magnetic chango produced by a
considerable change in spotted area is extremely small. We cannot
therefore regard the very large secular magnetic change as due to %
non-cunmlativo magnetic influence of some long-continued solar
variation ; nor does it seem possible to attribute the change to
solar influence at all unless we regard this influence as producing
results of a cumulative nature.
It is possible, however, to regard solar influence as producing a
cumulative effect in one of two ways, or by a combination of both.
For (1) time is necessarily an element in any influence acting upon
tlie hard-iron system of the earth — presuming the earth to possess
such a system. There are in fact indications in the results of § 82
that a system of tliis kind is perhaps connected, with the American
pole ; yet, even allowing the influence of time, it seems diliicult to
account for the peculiarities of the secular variation by an hypo*
thcds of this nature. But (2) any long-continued variation of solar
power would no doubt act cumulatively in producing an increase or
diminution of the large ice-fields round the poles of the earth. In
the course of time this cumulative change in the extent and dis-
position of these might perceptibly alter the distribution of tho
convection currents of the earth — and these, according to the views
lierein indicated, might in their turn perceptibly alter the earth's
magnetic system.
143. Concluding RemarJcs. — If we agree to look for an explanation
of terrestrial m^netism and its changes to strictly terrestrial pro-
cesses, we may derive some assistance in our search from such con-
siderations connected with symmetry as enable us, for example, at
once to perceive that when two peifectly similar things are rubbed
together we cannot have electrical separation, because there is no
reason why the one should be positively and the other negatively
electriBed. Suppose then that an observer stands at the equator
and looks towards the north, and then turns his back upon the
north and looks towards the south. In the first position let him
regard the northern system of meteorological processes and motions,
and in the second the southom. ^Tow if symmetry obtained abso-
lutely in these systems — that is to say, if the observer, whether he
regarded the northern or ihe southern system of things, had in
either case precisely similar phenomena at his right hand and at
his left — then wo should see no reason why the earth t^ould be a
magnet, or why one hemisphere should be the seat of magnetism of
the one kind rather than of the other. If then we regard meteoro-
logical processes and motions as being in some way the cause of
terrestrial magnetism, we must direct our attention to that peculiar
element which causes a want of perfect symmetry such as we have
described in meteorological phenomena. This element can hiutlly
be anything else than the rotation of the earth, wluch is fi-om left
to right to an observer facing the north, but from right to left to an
observer facing the south.
144. Now if we look upon the terre.<itrial meteorological system
modified by the earth's rotation as having protluced somehow in (he
past tho magnetic state of the earth, "it seems most natural to
regard the system which formerly produced this magnetic state a.i
being likewise that which at present nminUins it in its efficiency,
and which also accounts for the various magnetic changes which
take place. It would seem therefore that terrcstriul meteorology
and terrestrial magnetism are probably cognate subjects, and that
they ouglit to be studied together in the well-founded hope thftt the
phenomena of tho one will help us to explain those of the other.
Furthermore, if tlieso meteorological processes— deriving their
one-sided character from tho earth's rotation— aro to !)o regarded
as accounting not only for the origin but for the maintenance d'
the earth's magnetic system, we can hardly fail to imagine that
these processes must derive i>art of the energy which they exhibit
from that of the earth's rotation. Tidal energy we know is derived
from this source ; but we must likewise regard part of tlie energy
displayed in convection currents whether in the air or iu tho ocean
as derived no doubt from the same sonrci-. And wo may perhaps
allow that in tho phenomena of tidal action, as well as in those of
convection currents of tho nir and ocean, there may be, not merely
a transmutation of actual energy directly through friction into heat,
but likewise a transmutation of it, ultimatily p(-rha|»s into hiat,
but first through tho intermediate agency of electrical current.^
which serve to maintain tho magnetic state of the earth oud to
produce magnetic changes.
Now if this bo the case, if there be a large and compUcatod system
of tidal and convcrtion currents nil tending to change the rotative
energy of the eartli ultimately into heat, whether directly through
friction or indirectly through tho medium of cleclrieity, it is simdv
iuipossible with tlie present state of our knowledge to calculate with
the smallest pretensions to accuracy at what rate this transmutJition
is taking place, and hence at what rate tho velocity of the earth's
rotation is being slowly dimiuished. (B. ^
1»5
MET'H ODISM
I. ■Wesieyan Methotiism.
THE history of Wcsleyan Methodism embraces — (1) the
Methodism of Oxford, which was strictly Anglican
and rigidly rubrical, though it was also more than rubrical;
(2) the evangelical Methodism of the Wesleys after their
conversion (in 1738), tf which the Wesleyan doctrines cf
conversion and sanctification were tlie manifesto and
inspiration, while preaching and the class-meeting were the
great motive and organizing forces, — a movement which
before Wesley's death had developed into a form contain-
ing, at least in embryo, all the elements of a distinct
church organization, although in its general designation
and deliberate claims it purported to be only an unattached
spiritual society ; and (3) Weslcyan Methodism since the
death of Wesley, which, by steps at first rapid and after-
wards, though leisurely, distinct and consecutive, assumed
an independent position, and has grown into complete
development as a church.
1. Oxford Methodism. — This began in November 1729,
when John Wesley, returning to Oxford from Lincolnshire,
where he had been serving his father as curate, found that
his brother Charles then at Christ Church, had induced a
few other students to join him in observing weekly com-
munion. John Wesley's accession lent weight and character
to the infant association. Their first bond of association,
besides the weekly communion, was the common study of
the Greek Testament, with which they joined regular
fasting, the observance of stated hours for j)rivate devotion,
the visitation of the sick, of the poor, and of prisoners,
and the instruction of neglected children. They never
themselves adopted any common designation, but of the
variety of derisive names they received from outsiders that
of " Jlethodists " prevailed, — a sobriquet the fitness of
which, indeed, as descriptive of one unchanging and insepar-
able feature of Wesley's character (which he impressed also
on his followers), was undeniable.
This first Oxford Jlethodisni was very chmchly.
Between 1733 and 173C, however, a new phase was devel-
oped. Its adherents became increasingly patristic in their
sympathies and tendencies, and Wesley came much under
the influence of William Law. In regard to this period
of his history, Wesley himself says that he
" Iicnt the bow too far, by making antiquity a roordinato, ratlipr
tli.in a subnrJinJtc, rule with Sciiptuu-, by ailniitting several
tlonbtful wntinj^, by extending antiquity too far, by believing
more prarticoit to have been iniiversal in the ancient church than
ever were so. by not considering tliat tlic decrees of a provincial
fcynod could bind only that province, and the decrcca of a general
synotl only those provinces, whose representatives met therein,
th.Tt most of those doorecs were ad:ipted to particular times nnd
occasions, and, conscquf ntly, when those occasions ceased, must
ccaso to bind even tlioso provinces."
Tt was in 1736, during his residence in Georgia, whither
he had gone as a missionary of the Propagation Society,
that he learnt those lessons. Notwitlistanding his ascetic
severity and his rubrical punctilios, the foundations of his
High-Churchmanship were gradually giving way. AVhcn
he returned to England he had already accepted the
doctrine of " salvation by faith," although he had not as
yet learned that view of the nature of faith which he was
afterwards to teach for half a century. He had, however,
as in the journal of his homeward voyage he tells us,
learned, "in the ends of the earth," that he "who went
to America to convert others was never himself converted
to God." In this result his Oxford Methodism came to
an end.
The original Methodism of Oxford never at any one
time seems to have numbered as many as thirty adherents.
There was a set called "Methodists," hut there was no
organization, no common bond of special doctrine or of
discipline ; there were habits and usages mutually agreed
upon, but there was no official authority, only personal
influence. The general features of the fraternity, if frater-
nity it may be called, seem to suggest closer analogies
with the "Tractarian" school in its earlier stages than
with anything e'.sa in modern history, and the personal
ascendency of John Wesley may remind us in some measure
of the influence exercised a century later by J. H.
Newman. There was no more any germ of permanent
organization in the Oxford Methodism of 1735 than in the
patristic and "Tractarian" school of Oxford of 1833.'
2. Methodism after Wesley's Conversion. — John Wesley
landed at Deal, on his return from Georgia, on February
1, 1738. His journals on the homeward voyage, says
Miss Wedgwood,^ " chronicle for us that deep dissatisfac-
tion which is felt whenever an earnest nature wakes up to
the incompleteness of a traditional religion; and his after
life, compared with his two years in Georgia, makes it
evident that, he passed at this time into a new spiritual
region." r . ..." By Peter Bbhler,' in the hands of the
great God," he writes in his journal, " I was, on March S,
fully convinced of the want of that faith whereby wo are
saved." This " conviction " was followed on March 2-i of
the same year (1738) by his "conversion."
Like most good men of that age in England, Wesley,>
before he came under the influence of his Moravian teacher,
had regarded faith as a union of intellectual belief and of
voluntary self-submission — the belief of the creeds and
submission to the laws of Christ and to the rules and
services of the church, acted out day by day and hour by
hour, in all the prescribed means and services of the church
and in the general duties of life. From this conception
of faith the element of the supernatural was wanting, and
equally that of personal trust for salvation on the alone-'
ment of Christ. The work of Bohler was to convince
Wesley that such faith as this, even though there might
be more or less of divine influence unconsciously mfngling
with its attainment and exercise, was essentially nothing
else than an intellectual and moral act or habit, a natural
operation and result altogether different from the true
spiritual faith of a Christian. This conviction led him a
few days afterwards to stand up at the house of the Rev.
Mr Hutton, College Street, Westminster, and declare that
five days before he had not been a Christian. When
warned not thus to despise the benefits of sacramental
grace, he rejoined, " When we renounce everything but
faith and get into Christ, then, and not till then, have wo
reason to believe that we are Christians." It is true that
for several years after this he remained High-Church in
' One evidpneo of this is to be fonnd in the early and wide diverg^^
cnco of the varioTS niendjepi of the Oxfonl llethocbst company, after
thc-ir brief association at the university eanie to an end. We know
wliich way the Wv;sleys went ; we know also the separate path that
theirfriund Whitelield made for himself. John Clayton, the Jacobite'
churchiiian, settled at Manchester, renounced the Wesleys alter they,
btgaii their evangelical movement, and remained an unbending High-^
Chiirchnian to the end. Benjamin Ingham bceanic a gieat evangelist
in Yorkshire, founded societies, and, witli his societies or churches,
took the (leci-ive step of leaving the Cliunh of Enel.nnd and embracing
the position of avowrd Dissent. The saintly Garaliold, a poet as well
as a theologian and preacher, became a Jloravian biihop. Jainea
Hervey w.as in after life a famous evangelical clerBj-man, holding
" Low" and Calvinistic views. These were the chief of the Method.
isLs of Oxford.
« John ^Yestey and the Evangdical Rcactim of tlie 18M Century.
' A disciple of Zinzendorf, then iu Eusland on his way to Amerioo.
iU— a*
186
METHODISM
some of his principles and opinions, bat nevertheless his
ritualism was dead at its roots.
This experience also made Wesley an evangelist. He
h;id a forgotten gospel to preach, — the gospel by which
men were to be converted, as he had been, and to be made
" new creatures." And this result, this new birth, was
not dependent on any churchly form or ordinance, on any
priestly prerogative or service, or on any sacramental grace
or influence. To raise up, accordingly, by his preaching
and personal influence, a body of converted men, who
should themselves become witnesses of the same truth by
which he had been saved, was henceforth to be Wesley's
life-work. This was the inspiration under which he
became a great preacher ; this also made him an organizer
of his living witnesses into classes and societies. In the
pulpit was the preaching power ; in the class-room was the
private and personal influence. The vital link between
the pulpit and the class meeting was the doctrine and
experience of "conversion." Thus Wesleyan Methodism
is derived, not from Wesley the ritualist, but from Wesley
the evangelist.
Wesley's doctrines offended the clergy. His popularity
as' a preacher alarmed them. The churches were soon
shut against him. He attended the religious meetings —
on a Church of England basis — which had existed in
London and elsewhere for fifty years, so far as these were
still open to him, the Moravian meetings, and meetings in
the rooms of private friends, but these were quite
insufficient for the zeal and energy of himself and his
brother, who had been " converted " a few days before
himself. Accordingly, in 1739, he followed the example
set by 'Whitefield, and preached in the open air to immense
crowds. In the same year also he yielded to the urgency
of his followers and to the pressure of circumstances,
and, becoming possessed of an old building called "the
Foundery," in Moorfields, transformed it into a meeting-
house. Here large congregations came together to hear
the brothers. About the same time, m Bristol and the
neighbouring colliery district of Kingswood, he found him-
self obliged, not a little against his will, to become the
owner of premises for the purpose of public preaching and
religious meetings. Here was the beginning of that vast
growth of preaching-houses and meeting-rooms, all of them
for nearly fifty years settled on Wesley himself, which,
never having in any way belonged to the Church of
England, became, through Wesley, the Dossession of the
'Methodist Connexion.
The religious societies through which the Wesleys, after
their conversion, exercised at first their spiritual influence
were in part, as has been intimated, Moravian, —that in
Fetter Lane, of which the rules were drawn up by Wesley
himself in 1738 (May 1), being the chief of these, — :and
in part societies in connexion with the Church of England,
the successors of those Vhich sprang up in the last years
of the Stuarts, as if to compensate for the decay of
Puritanism within the church. In 1739, however, a strong
leaven of antinomian quietism gained entrance among the
Moravians of England (Bohler himself having left for
'America in the spring of 1738) ; and Wesley, after vainly
contending for a time against this corruption, found it
necessary formally to separate from them, and to establish
a society of his own, for which a place of meeting was
already provided at the Foundery. This was the first
society under the direct control of Wesley, and herein was
the actual and vital beginning of the Wesleyan' Methodist
Society, that is, of Wesleyan Methodism. Hence the
Wesleyans celebrated their centenary in 1839. It was not,
however, till 1743 that Wesley published the Rules of his
Society .By that time not a few other local societies had
been addd to tl\at at the Foundery, the three chief centres
being London, Bristol, and Newcastle. Hence Wesley
called his Society, when he jiublished the " Rules " in 1743,
the "United Societies." ilia brother's name was joined
with his own at the foot of these Rules, in their second
edition, dated May 1, 1743, and so remained in all later
editions while Charles Wesley lived. Those Rules are still
the rules of Wesleyan Jlethodism. Since Wesley's death
they have not been altered. During his life only one
change was made of any importance. In 1743 the offerings
given weekly in the classes were for the poor, there being
at that time no Conference and no itinerant preachers
except the two brothers ; after a few years the rules pre-
scribed that the weekly contributions were to go " towards
the support of the gospel." The Society is described as
"a company of men having the form, and seeking the
jjower, of godliness, united in order to (iray together, to
receive the word of exhortation, and to watch over one
another in love, that they may hull) each other to work
out their salvation." " The only condition ^jjrcviously
required of those who desire admission into these societies "
is " a desire to flee from the wrath to come, and to be saved
from their sins." The customary contribution was a
minimum of a penny a week or a shilling a quarter.
In 1739 these societies were not divided into "classes.";
But in 1742 this further step in organization was taken,'
and the change is recognized in the rules of 1743. Leadcm
were appointed to these classes, and became an order of
spiritual hel]-'ers and subpastors, not ordained like lay
elders in the Presbyterian churches, but, like them, filling
up the interval between the pastors that " labour in the
word and doctrine" and the members generally, and
furnishing the main elements of a council which, in
after years, grew up to be the disciplinary authority in
every " society." In every society there was from the
beginning a " steward " to take and give account of moneys
receTVed and expended. After a few years there were two
distinct stewards, one being specially appointed to take
care of the poor and the " poor's money," the other being,
in general, the "society steward.'' And, finally,— though
hardly, perhaps, during Wesley's lifetime, — in the larger
societies there came to be two stewards of each description.
The leaders and stewards together constituted " the leaders'
meeting," of which, however, the complete circle of funis
tions grew into use and into recognition only by degrees.
The Rules of the Society, which are strict and searching,
relate to worship, to conduct, and to the religious life, but
do not once mention or refer to the Church of England,
the parish church, or ihe parish clergy. The only authority
at first was the personal authority of the two brothers,
exercised either directly or by their ofiicial delegates.
After years had passed away the leaders' meeting came to
have an important jurisdiction and authority, but its rights
and powers were neither defined nor recognized until after
Wesley's death. From first to last there is no trace or
colour of any Anglican character in the organization.'
Moravians or Dissenters might have entered the fellow-
ship, and before long many did enter it who had either
been Dissenters or, at any rate, had seldom or never
entered a church. What would to-day bo called the
" unsectarian " character of his society ■was, indeed, in
Wesley's view, one of its chief . glories. All the timq,
however, this " unsectarian " society was only another
" sect " in process of formation. Wesley for many years
before his death had seen that, unless the rulers of the
church should come to adopt in regard to his society a
policy, of liberal recognition, this might be' the outcome
of his life-work. And it would seem as if in his private
confidences with himself ho had come in the end at times
to acquiesce in this result.
Still more decisive, however, was the tnird step in the
METHODISM
187
developoieiit of Wesley's " Society." The clergy not only
excluded the Wesleys from their pulpits, but ofte;i repelled
them and their converts from the Lord's Supper. This
was first done on a large scale, and with a systematic
harshness and persistency, at Bristol in 1740. Under
these circumstances the brothers took thecdecisive step of
administering the sacrament to their societies themselves,
in their own meeting-rooms, both at Bristol and at Kings-
wood. This practice having thus been established at Bristol,
it was not likely that the original society at the Foundery
would rest content without the like privilege, especially as
some of the clergy in London acted in the same manner
as those at Bristol. There were therefore at the Foandery
ilso sefjaratc administrations. Here then, in 1740, were
two — if we include Kingswood, three — separate local
churches, formed, it is true, and both served and governed
by ordained clergymen of the Church of England, but not
belonging to that church or in any respect within its
government. As thereafter during Wesley's life one of
the brothers, or some cooperative or friendly clergyman,
was almost always present in London and in Bristol for
the administration of the sacraments, these communions,
when once begun, were afterwards steadily maintained, the
Lord's Supi>cr being, as a rule, administered weekly.
Both on Sundays and on week days full provision was
made for all the si>iritual wants of these "societies," apart
altogether from the services of the Church of England.
The only link by which the societies were connected with
that church — and this was a link of sentiment, not an
organic one — was that the ministers who served tb^m
were numbered among its "priests."
In 1741 Wesley entered n\K>n his course of calling out
lay prcacher.t, who itinerated under his directions. To the
societies founded and sustained with the aid of these
preachers, who were entirely and absolutely under Wesley's
])crsonal control, the two brothers, in their extensive
journeys, administered the sacraments as they were able.
The helpers only ranked as laymen, many of them, indeed,
being men of hunlble attainments and of unpolished ways.
For the ordinary reccjjtion of the sacraments the societies
in general were dependent on the parish clergy, who, how-
ever, not seldom repelled them from the Lord's table. So
also for tlie ordinary opportunities of public worship they
often had no resource but the parish church. The simple
service in their preaching-room was; as Wesley himself
insistecf, defective, as a service of public worship, in some
im^iortant particulars ; besides which, the visits of the
itinerants were usually, at least at first, few and far
tetwecn. Wesley accordingly was urgent in his advices
'and iiijuiKtioMs that his societies generally should keep to
their imri.sli churchas ; but long before his death, esiiecially
'as the itiiii-'rant preachers improved in quality and increased
in number, ihcre was a growing desire among the societies
to have their own full Sunday services, and to have the
8.icranicnts administered by their own preachers. The
development of these preachers into ministers, and of the
nocictics into fully organized churches, was, if not the
inevitable, at any rate the natural, result of the step3
which Woaley took in order to carry on the work that waa
tontinuallv opening up before him.
In 1 1<4 Wusicy licM his finit Conference. The early Conferences
trore cliicdy iiK-fiil for tlic settlement of pointj of doctrine and
discipline and for tlio examination and accrediting of fellow-
labonrcre. Tlicy met yearly. Conferences were a necessity for
Wesley, and iKcanio inci ea»in<;ly so as his work continued to grow
ii|ion liim. It was inevitable also that the powers of the Conference,
Although for many years flic Conference itself only esistod as it
were on sulTeraiicc, and only cxctL-ised any authority by the per-
mfeion of its creator and head, ahonld coDtinoally inci-ea.se. Tlie
result u'xs that in 1784 Wesley could no longer delay the legnl
roH'-titution of the Conference, and that he was compelled, if he
vould provide for the perpetuation of his work, to take measures
for vesting in trustees,' for the iaf of "tho people callea Kethoa-
ista," under the jurisdiction of the Cooferenco as to the appoiut-
ment of ministers and preachers, all the prvaching places and trust
property of the Conneiion. The legal Conference wag defined as
consisting of one hundred itinerant jireachers named by Weslev,
and power was given to the " legal hundred " continually from the
first to fill up the vacancies in their own number, to admit and
expel preachers, and to station tliem from year to year, no preacher
being allowed to remain more than tliree years in one station.
By this measure Wesley's work was consolidated into a distinct
religious organization, liaving a legally cn.|x)rata character and
large property ri'jbts. And yet Wesley would not allow this greftt
organization to be styled a "church." It was only a "society"
— the "United Society" — the Society of "the people called Method-
ists"— the " Methodist Society." And of its mi-inbers all who
were not professed Dissenters were by him reckoned as belonging
to the Church of England, although a large and increasing pro-
portion of them seldom or never attended the services ot that
church. The explanation of this appfarent inconsistency is that
Wesley admitted none to be Dissenters except such as were so ia
the e}e of the law — those who, *'for conscience sake, refused to
join in the sci-viccs of the chnrch or partake of the sacraniente
administered therein " — and that he interpreted " the Church of
England " to mean, as he wrote to his brother Charles, " all the
believers in England, except Papists and DUsentcrs, who have tl>e
word of God and the sacraments ailministcred among them."
But Wesley waa to carry liii Society to a yet higher pitch of
development, and one which made it still more dilHcult to dis-
tinguish its character from that of a distinct and separate church.
In 17J8 Wesley had been theoretically a High-Churchman. For
some time even after he had entered ujion his conrso of irregular
and independent evangelism he continued to hold, in ti.e ahetrac^
High-Church views. But in 1746 he abaniloncd once for aU
bis ecclesiastical High-Churchmanship, although he never bccarao
either a political or a latitudinaiiau Low-Churchman after the
standard and manner of the IStli centur^y. He relates in his
journal under date Jairaary 20, 1746, how his views were rovolo-
tionized by reading Lord (Chancellor) King's account of tht
primitive (Aurch. From this time forward he consistently main-
tained that the " uninterrupted succession was a fable which no
man ever did or could prove. One of the things taught him J>y
Lord King's book was that the office of bishop was oiiginally oi*e
and the same with that of presbyter; and the practical infcrcncv
which Wesley drew was that he himself was a "Scriptural Episco-
pos," and that he had as much right as any primitive or missionary
bishop to ordain ministers, as his representatives and helpers, who
should administer the sacraments, instead of himself, to tba
societies which had placed themselves under his spiritual charga,
Tliis right, a* ho conceived it to be, he held in abeyance for nearlj
forty years, but at leu^h he was constrained to exercise it, an<(
by so doin^, in effect led the way towards makiag his Society a
distinct and independent church.
In 1784, the American colonies having won their indep^ndeace,
it became necessary to organize a separate Methodism for Americ3^
where Methodist societies had existed for many years. Wailey
gave formal ordination and letters of ordination to Dr Coke, alreadj
a presbyter of the Church of England, as sujierintendent ((^
bishop) for America, where Coke ordained Francis Asbury a*
presbyter and superintendent (or bishop), and Coke and Asbury
together ordained the American preachers as presbyters. From
that ordination dates the ecclesiastical commencement of American
Episcopal Methodism— in which the bishops are only chief among
the presbyters whom they snpcrintend, superior in office but of th»
same order. The Episcopal Methodism of America represents to-
day tlic largest aggregate of Protestant communicants and worship--
pcrs of the same ecclesiastical name to be found in any one natioa
in the World.
Tlie following year (1785) Wesley ordained ministers for Scot-
land. There his societies were quite outside of the establiiihed
Fresbyterianisni of the day, with its lukewarm " moderaiism ";
while the fervid sects which had seceded from Ihejtate churchl
would -hold no terms with Arminians like Wesley and his followers
Hence Wesley was compelled to make special provision for tha
admiiustration ot the sacraments in Scotland! Me therefor*
ordained some of his ablest and most dignified ]ireachers, wa»
careful to give them formally in his correspondence the style auJ
title of " Reverend," and ap^inted thftn to administer the sacra-
ments north of the Tweed. j_
At length, in 1783, Wesley ordained a number of preacher* (Mr
Tyerman says seven) to assist him in administering the sacraments
to the societies in Euglaad ; and of these he ordained one (Alexan-
der Mather) to be superintendent (or bishop), his brother Charlea
being now dead, and Dr CoUe sometimes abseut for long periods is
America. The number of societies which demanded to have- the
sacraments administered to them in their own places of worship
continually increased, and their claims were often too strong to
bo rcsLstil, espcci-iUj when the pariah prieet was eith« a pobliB
188
METHODISM
opponent of the Methodists or a man of disreputable conduct.
Roforo Wesley's dcatli (in 1791) it would scorn that tliciewcre more
than a dozen of hi-^ preachers who had at dilfcrcnt times, in Scot-
land or in England, been ordained to administer the sacraments.
^ Tho foregoing view of the development of Methodism as an
organization, durin;: the lifetime of its founder, will have conveyed
a general idea of its structure and polity. There is one cardinal,
though variable, element iu its organization, however, of which
there has as yet been no occasion to speak. The societies of
Methodism — each of these consisting of one or more *' classes " —
were themselves grouped- into circuits, each of which was placed
under tho caro of one or more of Wesley's Conference preachers,
who were called his "assistants" or "helpers," the assistant being
the chief preacher of a circuit, and the helper being a colleague
and subordinate. The "assistants" were directly responsible to
Wesley, who had absolute power over them, and exercised it
between the Conferences. The same power he etiually possessed in
tho Conference, at the yearly meetings, but he made it a rule,
during his later life, to take counsel with the Conference as to all
matters of importance alfecting the permanent status of the
preachers personally, or relating to the societies and their govern-
ment. He thus prepared the Connexion, both preachers and
people, to accept the government, and the legislative control of
the Conference after his death.
At the time of Wesley's death there were in Great Britain, the
Isle of Man, and the Cliannel Islands, 19 circuits, 227 preachers, and
67,562 members. In Ireland there were 29 circuits, G7 preachers,
and 14,006 members. There were also 11 mission circuits in the
West Indies and British America, 19 preachers, and 5300 members.
The number of members in the United States was returned as
43,265.
it has already becu explained that in connexion with each society
there was a leiders* meeting, of which society stewards and poor
stewards as well as leaders were members. It must here be added
that each circuit had its quarterly meeting, of which, at first, only
the .society stewards and the general steward (or treasurer) for the
circuit, in conjunction with the itinerant preachers, ^ere necessary
members. Leaders, however, in some circuits were very early, if
not from the first, associat«d with the stewards in the quarterly
meeting, or at least had liberty to attend. The quavterlv meeting
■was not defined in Wesleyan Methodism until the year 1852. The
leaders' meeting had no defined authority until some years after
"Wesley's death. Discipline, including the admission and expulsion
of members, lay absolutely with the "assistant," subject only to
appeal to Mr Wesley. Many years, however, before Wesley's death
it had become the usage for the " assistant," or, in his absence, the
"helper," his colleague, to consult the leaders' meeting as to
important questions either of appointment to office or of discipline.
As the consolidated " society " approached towards the character of
a "church," the leaders' meeting began to acquire the character
and functions of a church court, and private members to be treated,
in regard to matters of discipline, as having a status and rights
which might be pleaded before such a " court." The rights, indeed,
whicli, soon after Wesley's death, were guaranteed to leaders'
meetings and members of society had, there can be no doubt, so
far grown up, before his death, as to be generally recognized as
undeniable.
" Bands" were a marked feature in early Methodism, but in later
years were allowed, at least in their original form, to fall out of
use. There is no reference to them in the " Minutes of Conference "
after 1768, although till after Wesley's death they held a place in the
oldest and laigest societies. Originally there were usually in each
considerable society four bands, the members of which were collected
from the various society classes — one band composed of married
and another of unmarried men, one of married and another of un-
married women. All the members of society, however, were not
of neei'Esity members of bands. Some maturity of experience was
expected, and it was the responsibility of tlie " assistant " to admit
int'i band or to exclude from band. After Mr Wesley's death, where
" bands" so called were kept up, they lost their private character,
and bcrame weekly fellowship meetings for the society.
The "love-feast" was a meeting the idea of wliich was borrowed
from the Moravians, but which was also regarded as reviving the
pritnitive institute of the agape. In tho loi'e-fcast the members of
dilferent societies come together for a collective fellow.ship meeting.
Ojie feature of tho meeting— a memory of the primitive 'agape— \3
tlint all present eat a small portion of bread or cake and drink of
water in common.
It may bo supposed that in such a system as Methodism a large
number of preachers and cxhorters, from all tho social grades
Included within tho societies, could not but be continiially raised
np. T.nesi-, during Wesley's life, acted entirely under the directions
of tho assistant, and were by him admitted or excluded, subject to
an appeal to Wesley. Onco a quarter— often m conjunction with
the circuit quarterly meeting- a meeting of these local lay helpers,
called "load preachers," was held for mutual consultation and
yrangcmcnt, and to examine and accredit caudidales for Uio office.
3. Wesleyan Mcthodum after Wesley's Death (17^1).
— When Wesley died the Conference remained as the bond
of union and fountain of authority for tlie Connexion.
But between the meetings of Conference Wesley had acted
as patriarch and visitor with summary and supreme
jurisdiction. The first need to be supplied after his death
was an authority for tlie discharge of this particular func-
tion. In America Wesley had organized a system of
bishops (presbyter-bishops), presbyters or elders, and
deacons or ministers on probation. Among some of those
preachers who had been most intimate with Wesley there
was a conviction that his own judgment would have
approved such a plan for England. No document, how-
ever, remains to show that such was his desire. The only
request ho left behind him for the Conference to respect
was one which rather looked in another direction — tho
well-known letter produced before the Conference on its
first meeting after his death by his friend and personal
attendant, Mr Bradford, in which he begged the members
of the legal hundred to assume no advantage over tlie
other preachers in any respect. The preachers, accordingly,
in their first Conference after Wesley's death, instead of
appointing bishops, each with his diocese or province,
divided the country into districts, and appointed district
committees to have all power of discipline and directioa
within the districts, subject only to an appeal to the
Conference, all the preachers exercising equal riglits also
in the Conference, the " legal hundred " merely confirming
and validating jno forma the resolutions and decisions of
the whole assembly.
At first the preachers stationed in the districts were
instructed to elect their own chairmen, one for each district.
But the plan was speedily changed, and- the chairmen were
elected each year by the whole Conference ; and this
method has been maintained ever since. The " district
meetings"- — as they are generally called — are still "com-
mittees " of the Conference, and have ad interim its power
and responsibilities as to discipline and administration.
Originally they were composed exclusively of preachers,
but before many years had passed circuit stewards and
district lay officers came to be associated with the preachers
during the transaction of all the business except such as
was regarded as properly pastoral.
The relation of the Conference to the government of the
Coimexion having thus been determined, the question
which next arose, and which occupied and indeed convulsed
the Connexion for several years (1792-95), was that of the
administration of the sacraments, especially of tho Lord's
Supper, to the societies. The societies generally insisted
on their right to have tho sacraments from their own
preachers. Many of the Avealthier members, however, and
in particular a large number of the trustees of chapels,
opposed these demands. At length, between 1794 and
1795, after more than one attempt at compromise had
been made by the Conference, the feeling of the societies
as against the trustees became too strong to be longer
resisted, and accordingly at tho Conference of 1795 tho
" plan of pacification " was adojited, tho leading provision
being that, wherever the majority of tho trustees of any
chapel, on the one hand, ami tho majority of the stewards
and leaders, on the other, consented to the administration
of the sacraments, they should bo administered, but not in
opposition to either the one or tho other of those authorities.
In England tho Ix)rd'3 Supper was always to be adminis-
tered after the Episcopal form ; in Scotland it might still,
if nece.ssary, be administered, as it had commonly been
before, after tho Presbyterian form. In any case, howevc-,
" full liberty was to bo left to give out hymns and 'aj ".se
exhortation and cxlc.uporary prayer." Tho re.-"'!: was that
witbiu a generation the adJuiiniiitratico "l the sacraments
METHODISM
189
to the societies came to be the universal rule. By this
legislation the preachers assumed the powers of pastors,
in accordance, however, only and always with the desire
and choice of their flocks. No formal service or act of
ordination was brought tSto use till forty years after-
wards. All preachers on probation for the ministry,
after the completion of their probation, were "'received
into full connexion " with the Conference, this reception im-
plying investment with all pastoral prerogatives. Modern
Methodism has developed more fiilly and conspicuously
the pastoral idea.
No sooner was the sacramental controversy settled than
the further question as to the position and rights of the
laity came to the front in great force. A comparatively
email party, led by Alexander Kilham, imported into the
discussion ideas of a republican complexion, and demanded
that the members in their individual capacity should be
recognized as the direct basis of aU power, that they should
freely elect the leaders and stewards, that all distinction
in Conference between ministers and laymen should be
done away (elected laymen being sent as delegates from
the circuits in equal number with the ministers), that the
ministry should possess no official authority or pastoral
prerogative, but should merely carry into effect the
decisions of majorities in the different meetings. In the
course of a very violent controversy which ensued, pamphlets
and broadsheets, chiefly anonymous, from Kilham's pen,
advocating his views and containing gross imputations on
the ministers generally, and in particular on some not
named but distinctly indicated, were disseminated through
the societies. The writer was tried at the Conference of
1796, condemned for the publication of injurious and
unjustifiable charges against his brethren, and by a unani-
mous vote expelled from the Conference. In the follow-
ing year he founded the " New Connexion," the earliest of
the organized secessions from Wesleyan Methodism.
Views much more moderate than Kilham's prevailed in
the Connexion at large. At the Leeds Conference of 1797
the basis was laid of that system of balance between the
prerogatives of the ministers and the rights of the laity
which has been maintained in its principles ever since,
and which, in reality, has governed the recent provisions
(1877-78) for the admission of lay-representatives into the
Conference not less than the former developments of
Wesleyan Methodism. The admission of members into
the society had, up to 1797, been entirely in the hands of
the itinerant preachers, — that is, the "assistant," hence-
forth to be styled the "superintendent," and his "helpers."
The new regulations, without interfering vdth the power
of the ministers to admit members on trial, declared that
"the leaders' meeting shall have a right to declare any
person on trial improper to be received into society, and
after such declaration the superintendent shaU not admit
such p'erson into society " ; also that " no person shall be
expelled from the society for immorality till such immorality
be proved at a leaders' meeting. "^ For the appointment
of chiu-ch officers (leaders and stewards) the following
rejj.Jations were made, the second based on recognized
usage, the first on general but not invariable practice : —
' In this regulation it was assumed that the old rule of society by
■which a member disqualifies and vritually expels himself by con-
tinued absence from class, without reason for such absence, still
held good. The case provides only for expulsions for "immorality."
Subsequent legislation has introduced a provision which ensures to
any member before he ceases to be recognized on account of non-
attendance the right of having his case brought before a leaders'
meeting if he desires it. This rale of 1797 has always been under-
stood by the Conference as constituting the leadei-s' meeting in effect
a jury, leaving the superintendent with his colleague or colleagues
aradvisere to act as judge. Appeal has always lain from the leaders'
.meeting to the district meeting, and, finally, to the Conference.
" 1. No person shall bo appointed a leader or steward, or ho
removed from his office, but in conjunction with the leaders' moot-
ing, the nomination to be in the superintendent, and the approba-
tion or disapprobation in the leaders' meeting.
"2. 1116 former rulo concerning local preacliei-s is confirmed, —
viz., that no man shall receive a plan as a local preacher, without
the approbation of a local preachers' meeting."
The Conference at the same time made several provisions
for canying out the process, which had been going on for
some years, of denuding itself of direct responsibility in
regard to the disbursement of the Connexional funds.
The principle was established that such matters were to be
administered by the district committees acting in corre-
spondence with the quarterly meetings of the circuits. It
was also provided that circuits were not to be divided
without the consent of the respective quarterly meetings ;
and, finally, it was resolved that, in the case of any new
rule made by the Conference for the Connexion, its action
within a circuit might be suspended for a year by the
quarterly meeting, if it disapproved of the nUe. If, how-
ever, the Conference, after twelve months' interval, still
adhered to the new rule, it was to be binding on the whole
Connexion.
The powers of district committees, as defined by former
Conferences, were in 1797 confirmed and enhanced, special
powers being given to special meetings of these committees
convened when necessary to settle the affairs of a distracted
circuit. In the same Conference all the principal rules
of Methodism, in regard both to the ministers and the
laity, were collected and (in a sense) codified, in-iluding
the new regulations adopted that same year; and the
whole, under the title " Large Minutes," was accepted as
binding by the Conference, each minister being required
to sign hiS acceptance individuaDy. This compendium,
itself based on one which had been prepared by Wesley,
is still accepted by every Wesleyan minister on his ordina-
tion as containing the rules and principles to which he
subscribes. During the sitting of this critical Conference
at Leeds an assembly of delegates from bodies of trustees
throughout the kingdom was simultaneously held. The
form of the regulations enacted by the Conference was, to
a considerable extent, determined by the nature and form
of the requests made by this body of trustees. There
was one request, however, which the Conference distinctly
declmed to grant — namely, that for lay delegation lO iha
Conference. The Conference replied that they could not
admit any but regular travelling preachers into their body,
and preserve the system of Methodism entire, particularly
the " itinerant plan." It was not until many years after-
wards that anything was heard again as to this matter.
By the settlement now described the outlines of
Methodism as an organized church were fairly comjjleted.
Many details have since been filled in, and many changes
have been made in secondary arrangements, but the
principles of development have remained unchanged. The
Connexion after 1797 had a long unbroken period of
peaceful progress. The effect of the " Kilhamite " separa-
tion, indeed, was after 1797 not greatly felt by the parent
body. The number of Methodists in the United Kingdom
in 1796, the year of Kilham's expulsion, was 95,226; in
1797 it was 99,519 ; in 1798 the New Connexion held its
first Conference, and reported 5037 members, the number
of the parent body being 101,682. Nor was it till 1806
that the New Connexion reached 6000.
During the period of quiet growth and development whidi
followed 1797 the influence of one superior mind (Dr Jaboz
Bunting, 1779-1858) was to prevail with increasing sway. Thin
was to be the period of the gradual development of lay co-operation
in the administration of the various departniouts of Connexional
extension and enterprise^a development which prepared the way
for the important legislation of 1852 and following years, and for
the ultimate settlement of the respective provinces auti power*
190
METHODISM
of tlio roinistors and laity which was mado in 1877-78, It was
»lso to be tiio j>eriod of tlio f^radual completion of the pastoral
idea, in it3 practical application" to tho minijjters of the body.
TTiis period may bo dtlined as extending from tho revoUitionnry
opach of ]791-i'7 to the epoch of political and municipal reform
agitation, 182S-35, witich coincides with a second period of politico-
ecclesiastical agitation in Weslcyan Methodism.
In 1797 Iho Conference, as already mentioned, had rofnsed to
allow elected laymen — or lay delegates — any place either In tho
Confereuco or in district committees. Witliin u few yeai-s after
ISOO, however, tho practice grew up for the circuit stewards to
attend tho district committees during the transaction of financial
business, and in 1815 this usage wiis recognized in tlio Minutes of
Conference as an ostibiishcd "rule," and it was enacted that no
general incrca.se of tho income of the ministers should be sanctioned
by tho Conference until approved by a majority of the district
eoraraittees during the attendance of tho circuit stewards. Since
tho adoption of this rule tho lay olemout in the district committees
has steadily increased and devuloped. Another characteristic mid
important feature in tlie organization of "Wcsleyan Methodism,
which grew into distin :t form and prominence -during the poriotl
now under review, was that of the administration of all the Con-
noxioiial departments, except such as were regarded as properly
pastoral, by iheans of mixed departmental committees, appointed at
each successive Conference. These committees made rocoramendti-
tions to tho Conference in regard to such new legislation as they
thought desirable and to the appointment orthe members of com-
niittoe; and, for each department, a large committee of review, of
which the membera of the ordinary committee of management
formed the nucleus, came to be held each year immediately before
tho Conference. In these committees the numbers of ministers and
of laymen were equal. On this principle, between 1811 and 1835,
provision had been made for the management of all the funds of
tho Connexion and their corresponding departments of administra-
tion. Tlie Jirst mixed committee appointed by the Conference was
tho committer ot privileges in 1803.
The development of the pastoral position and character of the
ministers of the body after 1797 could not but advance on a line
i-arallel to the development of the position and claims of tho
laity. In 1818 the usage of the Conference was conformed to what
had long been tho ordinary unofficial custom, and the preachei-s
began to be styled in tho Wcsleya7i Methodist Magaziiie and in
other official publications *' Reverend," a fact which may seem
tiivial, but which in reality was of important significance.
In 1834, after tho idea had been long entertained and the project
had been repeatedly discussed, it was determined to establish a
theological institution for the training of ministerial candidates.
There are now four colleges, with two hundred and fifty students.
In 1836 the practice of ordination by imnosition of hands was
Adopted.
Such advances, however, as these in the general organizatiDn
and development of the Connexion, and especially in the status
and professional training of tho ministers, could not be made in
such a body without olfcnco being given to somo, whose tendencies
were to disallow any official distinction between the ministry and
tho laity, and who also objected to the use of the organ. This
levelling clement wa-i strong in the West Riding of Yorkshire, and
in 1828, on the placing of an organ in Brunswick Cbapol, Lccds^
by the trustees, with the consent of the Conference, a violent
agitation broke out. The ponsequence was a disruption, the first
binco 1793, under the title "Protestant Methodists." But this
wa:^; absorbed, eomo yeara later, in a more considerable secession.
In fact, tho Connexion was in 1828 entering on a period of agita-
tion. Tho current of political affairs was approaching the rapids of
which the Reform Act marked the centre and the point of maximum
nmvemcnt. A body like Wesloyan Methodism could not but feel
in gioat force tho sweep of this movement. It is true that Wesloyan
Methodism as such has never been political, that few of its numbers
cultivated extreme politics, and that the ministers and tho better
classes of the " Society " were strongly Conservative in their general
tone. NcvortheloRs the mass of the community shared m tho
giineral movement of the times, and tho Conservative tone of tlie
ministers ami of most of tho well-to-do laity was not in full har-
mony with the sympathies of tho people generally. Acconliugly
the elements of disturbance, which only partially exploded in the
" I'rotestant Methodist" secession, continued to mafto themselves
felt, in dillcront parts of tho Connexion, duriu" tho following years
of political controversy. The decision of the Conference in 1834 to
provide a college for the training of ministerial candidates gave
special ofTouco to tho malcontents. Such an occasion was all that
w;is wanting for tlio various discontents of the Connexion to gather
to a head. Tho domauils made by tho agitators proceeded on a basis
of domocratic ecclesiasticism such as it is very difficult to apply suc-
cessfully to a system of associated churches. The result was a third
soccssion, based on the same general ground of ercle-^iastica! prin-
cinles as tlie two preceding, which was organized in 1836, and with
.wliich tho "IVotostant Mothodistii'* eventually (.oalcscud. This
now secession was known first as the '• Wesloyan Methodist Associa^
tion " ; but for a number of years past it has been merged in a still
larger body of soccders designated "Th« Methodist Tree Cburcheb."
Its leader at tlie fii-st was the Rev. Dr Warren, who left it, however,
not many mouths after it was formed, and took orders in the Church
ofLngland.i
The controvorsios of 1835-36 left their mark on the legislation
and official documonLs of tho Connexion. The princi|des of 1797
remained intact, somo farther guards only being added to prevent
any (hnj;cr of hasty or irresponsible action on the part of super-
intendents, and at tho same timo "minor district meetings*' being
organized in order to facilitate appeals. One error was, liowever,
committed by the Conference. In 1797 no provision ha»l been made
for bringing the circuit, through its quarterly meeting, into direct
relations with the Conference. In 1636 a right of direct memorial
to the Conference was ijiven to the circuit nmirtcrly meeting; but it
was so fenced round witJi conditions and limitations as to make it
practically inoperative, and at the same timo provocative of sus-
picion and irriUtion.
Tiio efl'ect of the secession of 1836 on the general progress of the
Connexion was not great. The number of members icported iu
1835 in Great Britain and Ireland was 37l,2iil (tlieio being a
decrease in England of 951), in 1836 381,369, in 1837 384,723. For
tho next ten years the advance of the Connexion in numbci-s and in
general prosperity was apparently unprecedented. Tlio Centenary
Fund of 1839-40 amounted to £221,000. In the midst, however,
of all the outward prosperity of Methodism — partly perliaps in con-
sequence of it — very perilous elements were at work. The revolu-
tionary ideas of tho Chartist period (1840-48 and of Continental
politics (1848-49) reacted on Wesloyan Methodism us the political
ideas of 1791 and of 1831 had done at those epochs. The embers
of old controversies — ecclesiastical. qua'^i-]>olitical, and personal —
still smouldered, and at length burst into fresh flame, jprom 1844
a stroll" spirit of opposition to the leaders of tho Connexion, and
especially to Dr Hunting, was fanne<l by the circulation of anony-
mous "ny leaves" of a very scurrilous character. At the same
time the policy of the Conference and of the ministers in their cir-
cuits had proceeded more than was wise on the old lines. The
general administration relied too much on the footing of implicit
confidence on the part of the peojilo and on the power of official
prerogative in the hands of tlio minister. The memorial law of
1836 was indicative of the too exclusive spirit of pastoral govern-
ment which liad prevailed. The wistlom of Dr Bunting Lad Tor
five i^nd twenty yeai-s led the way in giadnally liberalizing boththe
polity and the jiolicy of Methodism, and adapting them lo the
clianging conditions of the times. But this wisdom seems to have
found its limits before 1849, when the internal dissensions reached
their climax. In that year James Everett, the chief author of the
fly sheets, and two other ministei-s, Samuel Dunn and William
Griffith, who had identified themselves with him, wero expelled.
A disastrous agitation followed. No distinct secession took place
till after tho Conference of 1850. Tlie union of the "Methodist
Free Churclies," in which was incorporated the *' Wesleyan
A.ssociation" (of 1836), was formed by the scceders. The "I^cw
Connexion" also received some thousands of the seceders into ite
ranks. But by far the greatest part of those who left went with
neitlier of theso bodies.
Between 1850 and 1855 tne Connexion in Great Britain and
Ireland lost 100,000 members, and not till 1856 did it begin to
rei'ovor. In that year the numbers were returned as 282,787,
showing a small increase over the preceding year. Since then peace
and unity have prevailed unbrokeu.
The convulsion of 1849-52 taught the Connexion, and in par-
ticular the Conference, lessons of the highest importance. In 1852
the quarterly meeting was so defined as to make it the gieaf repre-
sentative meeting of the circuit, includiug stewards, leaders, local
proachei-8, and trustees. Tho right of memorial to the Conference
was given to it in the widest ond fi-eest sense. These powerful
bodies invite ministers to the circuits, or decline so tu do, deter-
mine and j)ay their "allowances," as s-darirs to ministers are still
called in the Connexion, and review all the interests of tho circuits,
spiritual or financial. They had niso conferred ujion them in 1852
tne right to appoint a circuit jury of appeal from the verdict and
findings of a U-atJeis' meeting in certnin cases of discipline. Since
1852 Conferenco legislation lias still proceeded in tho direction of
recognizing and enlarging tho functions and rights of the laity.
Tho committeo of review system, already spoken of, had been con-
siiieraldy developed between 1835 and 1849, and included every
department of ordinary administration. Iu 1861, however, whilat
a representation of tho departmental executive committees fonned
still the leading element in each committeo of review, a great im-
provement was made in their constitution by giving to o»eh of the
districts of British Methodism tho right to send a lay pepreeentativo
> This " Wnnciiitc" sccraslon. as altlnt It wii» comiiionlv ciiIlelKl»^« rto to •
Ittw-uit wlikh led to tlio JtuUclAl rcrocnUloii l.y ilic Ctuir; of Chsncrry of th©
Conforcnco Died Poll of 1781. mid llie - UrRP Mlnulcs" of I7W. a» ilocumoota
having tho foi-co of public luvr In llio uliululdtriLUon of Wesloyan MotliudlJiii.
M E T H 0 D'l S M
191
lo .ittend tliese preparatory Conference committees. lu 1877 and
1S7S tlie final and natural coiismnniutiou of tlic whole cour^sc of
Rtlvaiice since 1791 was clVerted in tlio constitntiou of the uniti^d
Conference of ininistertiand hiy rciuvbi-ntativi-s. The niini:>tfi-s nicit
l>y tlicn«!clves to discharge the lunetions which Lclon;^ to thuiii
as the coniMioii pastoiatu of the Connexion. As to all tlie ixiiuis
involved in ihcir spccilic cliaracter and common retiponsibility, as
the niutnally exchanging and itinerating pahtor.t in foniniun uf a
'vast coninion Hock, they lake mutual couii.-icI in a srjiaiatu asstinhly.
ThoConfcivnce, in it^ miuistc-rial-and-lay or ruprcsjntative si.>s<>ion,
meets it Iter the pastoral Liu:»incss i^ cohiiileted, and occupies a lull
week bctwctn Sundays in diacussing and st-ttling the busincbs o!
all the funds and the gvufrul adniiiiislrativc d'jpartincnrij of the
body. The CoiikMciice in its pastoi-al session as^cniblcs on the Iniit
Tuesday in July, tliat ses-sinn closing on the l-'riday or Saturday
week following; the ruprcscntitive session occupies the lollowing
week. It is legally necessary that the decisions of the Conference
in both its scssiuns should be contiruicd and validutvd by the vote
oif the "Icg.d hundred." This conlirmatiou is, however, n'veu om a
matter of couise.
The Coufcicnce in its jiastoral session is not formally rcpn-senta*
five. To each di:strict is assigned by the lueecding Cimlcrencc a
rertaiu amuuut of rcprcscntudon, tlieru being at present tliiitylivc
districts. Tlie uunibcra allocated to the districts vary according to
circumstances. The total number of ministers and laymen com
pofting the Conference in its representative session is 48ii, or 210
ministers and 240 laymen. The basis of the lay representation in
the Conference is tlie constituency of lay olficials in the district
committees. The Connexion at large is rcpirsentcd by the lay
officials of *I.e general Connexional di-partmcnts. The business
tninsiict .» in tlie Conference duiiiig its representative session re-
lates to all the Connexional dc|iartnicnt3 of general adniinistralion,
viz., the committee of privilcgi s, foreign ndssions, the mainlenance
and education fund (and the schools) lor ministers' children, chapel
alfairs (general, metropolitan, and ]iroviucial}, the Ironie mi»it;n
aud contingent fund, district sustentation funds, armv and navy
evangelization, lay mission work, the worn-out niitiistcrs' antl
ministers* widows' fund, the theological institution with its four
colleges, Sunday and day sclionis and the cliildrcii's home and
orphanage, higher education, the extension fund of Mcth(.disni,
alterations and divisions of circuits and districts, and the Lord's
Day observance and teuijicranec tpicstions.
The president of tlie Conference is chosen by the ministers hy
ballot on the openiirg of the pastoral session. After the rlectiou
of president follows that of secretary. These elections, however,
cannot take place until the vucancies in the h<in>lred have been
filled up. Such vacancies arc caused by death, by absence lor two
ycai-s together without a dispensation, by expulsion, or by super-
annuation, which Ukc9 place ordinarily after two.years' retirement
from the full work of the niinistry.
The ]>rincipal Matistics of the denomination at the last Confcren^'c
(1882) were as follows :—
'
Mcniljcr».
On
>linlstcn>.
On
TiUil.
Ilollioil
orSii[x;i--
Suiuloy
SclioUi..
Qivat lliittiin
09-1,764
•.M,471
40,C.',1
77C
12.034
1,649
•iOO
34?
81
IX
193
279
IG
82P,0CC
foreiKH n)l-«ion».>
Of tlie Sunday echolai-s in Great Uritain, 177,965 wcro over
fifteen yeara of age, aud 93,127 were meinbcis of society or ou
tl-ial OS members.
WesUynn Afft/iodism in Ireland has always been part and parcel
3f British MetlioJism, but since 1782 it has had a branch Confer-
ence of its own. 'I'ho acts jf this Conference are, in accordance
with a pi-ovision in the Coufcrcnco Deed I'oU, made valid by tho
-oucurrcnce with thcru of a dch^-ate from tho British Conference,
*ho is to tlic Irish Conference wliat the legal Contcrcnce is to the
British Conference. Ten ministera of the Irish Conference are
nioinbora of tho "liRal hundred" of the British Conference. The
'*plaii of pacilicatioM " of 1795 was not carried out at the time by the
in»h Conferenco. In the year 1816, however, it was adoiitcd in
(rcland. The result was a secession which assumed the designation
" Primitive Wcsleyans," a very dilfcrent body from the rrimilive
Methodists of England. In 1878 tho Primitive Wcsleyans were
reunited to the parent Conneiion. The number of niembci^ in
.roland has, owing to emigration, not increased of late years. The
ast return showed 24,475 members. * '
A^liatcd Conferences. — For more than twenty years there were
Several "affiliated Conferences" of British Methodism. IJut there
ire now only two— the French Methodist Conference, and that of
fiovth Africa,— the latter constituted quite recently (1882). Since
1852 French Methodism has been under an affiliated Confcicnce.
The dimensions of the French Connexion, however, arc very small,
anU it^ dependent to a considei:able extent ou pecuniary aid fur-
IXUefljr In Uie West lodles, Africa, India, and Cbiiuu
nishcd by the 'Wesfcyan Missionary Society. The last statistical
return showed 1769 membeiTj, 126 membeiTi ou trial, 27 ministers,
1 minister on trial, and 3 suiicmumcrary or retired ministers. Tho
British Conference has a right of veto as to certain |ioints of legis-
lation in the case of alliliated Conferences.
Atu>irulasiaii, Mctkadixm \\si% iot more than twenty years under
an aHiliated Confci-ence, dating from 1854. Since 1876, however,
the Australasian Ccnfeicnce has been independent. The General
Conference meets once in thieve yeai^, having under it our annual
Conrcrenccs— one for Kew Soi.th Wales and yyccnsland, another for
Victoria .and Tasmania, a tliird for Soutli Au^>tralia, and a fourth
for New Zealand. These Conlcrciices— the general and the annual-
are all mixed and represent.irivc after the same general pattern aa
the liritish Conference. The have also under their charge, and as
jiart of their Connexion, the ".Ve»lejan missions in Tonga'and Fiji,
wliich were begmi by tho parent bg.ly before the original affiliated
yearly Confcicnce for Australasia was or''anized. The unmbers in
1881 were for the Jkthodisni of Australia 28,310 members with
ZGi ministers, and for the SouUi Sea missions 33,411 members with
16 missionaries of Euroiican Wood and a very large number of
native ministers and assistant iiinistci^
Ciiiiniliitn UelhoKlisiii was aho alliliated till 1873, when it became
an imlepemlent Connexion. Ii includes six |iroviiKial annual Con-
ferences and one General Conference which meets every three years.'
The General Conference is mijed and reiuesentative ; the annual'
Conferences are jiurcly niinisteiial. Canadian Methodism occupies
a |io«erlhl position in tlio Dominion. It numbers as nearly as can
bi' ascertained about 116,000 nicmbers,, and is strongest in Upper
Canada. It possesses a university — the Victoria Uuiversity in
Upper Canada.
The Doctrines of Methodism. — In doctrine all branches
of Jlethodism are substantially identical. Wesley's
doctrines are contained in lifty-three sermons known as'
the " four volumes " and in his Notes on the Xew Testament.^
The Conference has, however, iiublislied two catechisms,'
one for younger the other for older children, of which a'
new and carefully revised edition has lately been completed.^
In general, Wesleyan theology is to bo described as
a system of evangelical Arminianism. In particular,
Wesleyan divines insist on the doctrines of original sin,
general rcdeiliption, repen,ance, .justification by faith, the
witness of the S[iirit, and Christian perfection, — or, as it
has been eiistomaiy for Mctliodists to say, the doctrines of
a " jirescnt, free, and full salvajtion." liy the witness of
tlic ypirit is meant a consciousness of the Divine favour
through tire atonemient of Jesus Christ. Wesleyans have
often been represented as holding the Calvinistic doctrine
of "assurance." The word, however, is not a Wesleyau
lihrase, and assurance, so far as it may be said to be taught
by Methodists, signifies, not any certainty of final salvation,
but merely a " sense of sin forgiven." ^
II. American Episcopal Methodism, v
The beginnings of American Methodism are traceable to
the year 17CG, when a few pious emigrants from Ireland
introduced Methodism into New York. Ou receivin" an
ajipeal in 17G8 from the New York llethcJists, who were
engaged in building a preaching-house, Wesley laid the case
of America before the Conference at Leeds in 1769, and.
two preachers, Boardman and Pilmoor, volunteered to go
to the colonies. Boardman went to New York, Pilmoor
to Philadeljihia. In 1771 two other Methodist itinerants,'
Franv.i3 Asbury — the most famous name in American
Methodism — and Richard Wright, went out to America.
In 1773 Thomas Rankin, a preacher of e.xiiericnce sent out
* Besides Wesley's Sermons and Soles, llis Appeals and hi* Irc.ntlse on Oiioinat
'Stn, in reply to Dr Taylor of Noi wich, should t>c ri-ud in on\cr to jiiipi ed;ite his
thcolocical vievs. After tiicse may be partlfulaily mitcd Jnse|ili Hi*iis<'n"s
Commentary, Watson's Institutes (3 voN.X I)r Pepc'a Compendium of Ttietilu<j>f
(3 vols.), the series of Fernleij i«turrt espiclally that by llie Rev. H. Gregory ou
"The Holy Catholic Cliwcli," and Dr Itlcg's />wci)«rMi and Addresses.
* For the history and constltutlo'n of Weslcj-an Merhodlym tl-c foIhiwinR wotks
may be consulted: — Wesley's Woik". especially his Jovmals; Soutlicy's Wesley;
Tycrman's Wesley, RIrk's Lictrlg Weslfy, auil Clturchntansliip of Jolin Wesley;
Jackson's Life of Charles Wesley; Minutes of Conference, vol. 1., 1744-98; I).-
Gcorce Smith, History of Wesleyan itetliodism.Z rola.; Dr Abel SIcvi-iis, J/ts/ory
of Urthodism. 3 vols. ; Pierce. Polity of Methodism ; Di- Wllliums. Constitution
and Polity of Wesleyan Metltoditm : Bi^, CsnnexivntU .Jkonomy; and the
Minutes, 1877 (o 1881,
192
METHODISM
by Wesley, held tBe first Conference in Philadelphia, when
;here were 10 itinerant preachers and 1160 members.
\fter the breaking out of the War of Independence the
English Methodist preachers were unpopular, and all but
Franeis Asbury went back to England. At the end of the
H-ar, however, in 1784, Wesley sent out Dr Coke, and
American Methodism was organized as an independent
church, with Dr Coke and Francis Asbury as its presbyter-
bishops. The history of American Methodism since that
period is too vast and complicated for any attempt to be
made to summarize it here. Methodism is more properly
national in its character as an American church than any
church in the States. In Massachusetts and some other
of the New England States it is less powerful than Con-
gregationalism, which still retains there much of its ancient
predominance ; in the city of New York it is less powerful
than Presbyterianism, and, indeed, occupies a position less
generally influential than might have been expected. But
m Philadelphia it is very powerful ; so also in Baltimore
and in Cincinnati ; if not strong in New York city, it is
very strong in the State ; and generally throughout the
western and mid-western States it is the prevalent form
of faith- and worship. In the south, also, it is more
powerful than any other church.
Ameiican SIcthodism is Episcopal. But its Episcopacy is neither
prelatical nor diocesan. Tlie bisliops are superintending presbyters,
and they visit the whole territory of Slethodism in rotation, hold-
ing (presiding over) the annual Conferences. These Conferences are
purely ministerial. But the Ueiieral Conference, which meets once
in four years, and which is the Conference of legislation and hnal
appeal, is mixed and representative. The first General Conference
was held in 1792, the first delegated or representative Conference
in 1812, the first mixed or niinisterial-and-lay General Conference
in 1872. There were till lately no district assemblies in the
Episcopal Methodism of America, and nbw there are but few. The
bisliops maintain the unity of the Connexion in the interval between
ihe General Conferences, by their visitation and by their conjoint
council. A sub-episcopal class of ministers also, called presiding
elders, supplcmeht the action and superiiiteudency of the bishops.
These preside over districts, holding all the circuit quarterly meet-
ings, and holding the district meetings, if any such meetings have
been organized,
American Episcopal Methodism is distributed into five distinct
sections or chuichcs, which, however, differ from each other in no
points of any importance as rcsjieets organization or discipline, still
less doctrine. The American ilethodist Episcopal Church South
became a separate organization in 1847 by reason of the slavery
controversy. Tlie coloured churches, of which there are three,
sprang U[i distinctly from local causes. The following are the latest
available statistics: —
Itinerant
Mhilstcis
Loral 1 Ly 1
I'reaclicrs. Members.
Mil r t F i pon 1 Church
12.Hi
4,001
:.8.1i
1,650
(l.'iS
12,3i3
S,S68
0.7C0
3,7o0
C83
l.TH.-W?
837.K3I
391 ,044
300,000
112,000
Mctliodisl Episcopal 71i>li Church
Coloured Mclliodkt Episcopul Churcli
20.2Cli
3-',3»4
3.3-W,H2
In the Methodist Episcopal Church alone there are one hundred
annual Conferences, visited by twelve bishops. This church lias
Iiioro than twenty universities, of which some arc distinguished
schools of learning. Hostoii University is one of the most recent and
one of the chief. The principal foreign missions are in India, China,
and Japan. The Methodist Cliurih South also has some infltiential
universities, particularly that at Nashville, and has missions, in
particular in Japan and China.
1 Besides these Mcthoilist Eiiiseopal churches, with their total of
3,3,'')8,000 church memhera, there are two other churches which do
not a.s3umo the name at all, but are yet essentially Methoilist in
doctrine and disciidinc, not varying in any important particulars
from the Episcopal Methodism of America. Of these one is called
tho United Brethren, with l.''i7,000 members, the other the Evan-
gelical Association, with 113,000 members,'
Non-Episcojml American MctkorUsm.—lho bodies included under
this lieail are cliielly secessions from tho original stock of American
Methodism, founded on principles ofdeniocratic church government,
analo^-ous to those of tho English Methodist secessions. The only
) Atncrlciin Methodism Is Hr Abel SIcvcns'n MiKory.
I Klvcn In tho UWMilitl.Yar Doat, Mow Vork, 1SS2.
considerable body, however, is the Methodist Protestant Cburcb>
with 12.'>,000 members. The minor bodies, four in number, count
altogether less than 60,000 members, the principal being tha
American Wesleyan Cliurch, with 25,000 members.
III. Other Methodist Bodies in Britain.
The bodies still to be noticed, while differing as tb
points of church government, agree as to doctrine and
in general as to the means of grace and as to inner spiritual
fellowship with the parent " Connexion." They all
maintain class-meetings and love-feasts, have leaders'
meetings and quarterly meetings, and largely employ local
preachers.
The Mclhodiit New Connexion was founded in 1797-98 by
Alexander Kilham, who died in 1798. Its general principles are
inilicated above. Its 'statistics for 1881 were as toUows:— 183
inini.iters and 27,770 members (including those on mission stations,
besides 3882 on trial), and 74,744 Sunday scholars.^
United Methodist Free Churches. — This organization in its original
form must be identified with the Wesleyan Methodist Association
of 1336. That body first absorbed into itself, in great part, the
" IVotestant iMethodists" of 1828. It was afterwards greatly in-
creased, and its organization in some points modified, when a large
number of the scceders flora the parent Connexion in 1850-52 joined
its ranks. The main body of its Conference does not consist, like that
of the New Connexion, of an equal number of circuit ministers and
cLci-tcd circuit lay delegates, but of circuit delegates, whether
ministerial or lay, elected without any respect to oltice, ministerial
or other. Its circuits also are independent of tlie control of the
Conference. The Connexional bond, acconlingly, in this denomina-
tion is weak, and the itinci'ancy is not uuiversal or uniform in its
rules or its oi>eration. The amalgamation between the Wesleyan
filcthodist Association and tlio " Wesleyan Jlethodist Reformeis"
of 1850 took place in 1857. At that time the combined clmrches
numbered 41,000. At present (1881-82) they number 72,839, in-
cluding 7772 members ou the mission stations, besides 7824 on trial.
The number of ministers is 392, with 40 retired or '* supernumerary"
ministers. The number of Sunday scholars is 190,957.'
Primitive Mcthodibvi. — In this earnest and hard-working denomi-
nation the ministers, of whom some arc woineii, are very literally
" tlie servants of all." The Conleience is composed, in addition to
twelve permanent members, of four members appointed by^thc pre-
ceding Conference, and of delegates from district meetings. The
jii-inciple of in-ojiortion is that there should be two laymen to one
minister or '* travelling preacher," and the *' travelling preachers"
have no pastoral prerogative whatever. The Conference is supreme^
and the Connexional bond is strong. Tliis body was founded by
Hugh Bourne and William Clowes, local preachers who were
separated from the Wesleyan Connexion, the former in 1808, the
latter in 1810, because oftheir violation of Coiiferenco regulations
as to camp meetings and other questions of order. The Conference
hail, in 1807, luonounced its judgment against cainp meetings,
which had lieeu introduced into the country fiom America, whcr<a3
Bourne and Clowes were determined to hold such . meetings.
Founiled thus by zealous and " irregular " lay preachers, " Primi-
tive" Mi-tliodisin, as the resulting new body called itself, bearsstill
in its organization, its spirit, and its customs strong traces of its
origin. It has been a very successful body, aiming simply at doing
evangelistic work, and is now numerous and powerful, iiuiubcriiig
among its ministei-s, not only many useful pi-eacliei-s, but some of
marked originality and iiowor and also of superior cultivation.
Tlieio li.TS for many years jast, if not from the beginning, been a
very friendly feeling between tiic old W cslcyau Conncvion ami the
Primitive Methodists. Its latest statistics (18S1-2) show 1H9
travelling preachers, 185,312 members, and 383,350 Suii.lay
scholars.*
Bible Chridinns.—'T\\e Primitive Methodists snrang «p in tho
midland counties, the Biblo Christians in Cornwall. These closclj
rcsembic the " Primitives " in their character and spirit. Their
founder was a Cornish local preacher called O'Bryan. Hence tho
Connexion is often known as the Bryanites, and Cornish emigrants
have proiiagated this deiioniinalion widely in the colonics, Tho
Confciciico is composed of ten superintendents of districto, tlio
president anil secretary of the preceding Conference, lay delegates,
one from each district meeting, and as many of tho travelling
preachers as arc allowed ly their respective district n>cctin"s to
attend. In general it may iie said that the ministerial and lay
memhcrs of the Conference aie about equal in number. Tlio returns
for 1881-82 showed in England (chielly the west ami south of Eng-
' Soc Jmbltf Volumt c/ Iht Stic Comriian: nlso tho 0.-»»™( ff«(#j ud tho
ir.ntilnofCmr'rtnn. ISSI. P"bll^h>•J «l II* Nc-. Coi>ncxl"n Uooknooiti
3 S-c A'o««./..(.oi. /v-J 1./ II'' VniM ilclhoaiil Fif Cturrhn; aiso Uivkia
« Seo Jnim roue. «i</."» «/ '*• I'rujnlln U,ll,oJill CMmuicn : tlto Udiula
0/ Con/tract, 1»SI, 6 smtun Sirocl, London, E.
METHODISM
land) and in the Channel Islands 186 itinerant preachers, 21,209
members (besides 690 on trial), and 36,335 Sunday scholars. In
Canada the number of members was 6052, and in Australia and
New Zealand 3671. >
The IFcskyan Reform Union is an aggregate of local Methodist
secession churches, loosely held together by a Conference, arid is
one of the results of the great Methodist disruption of 1851-52.
The returns for 1831-82 showed 18 ministers and 7728 members.
(Ecu^ncniml Mclhodinl Conference. — This Conference was held in
CSty Road Chapel, London, in September 1831. Representatives
were present from all the Methodist bodies throughout the world,
and it was estimated that these represented not less than 5,000,000
of members and 20,000,000 of population. Whilst in chiuch
organiiation these bodies differed, as has been shown above, in
doctrine and in respect of their purely spiritual discipline and
means of grace, they were all agreed in principal matteiB. Tlio
Conference was entirely practical in character. The object was to
promote zeal and union among the constituent bodies as to all
practical points of Christian sympathy and activity, at home and
abroad, and especially as to home mission worlt, general philan-
thropy. Christian education, and a Christian use of the press. There
were 400 representatives present from the Methodist bodies in all
parts of the world.^
Welsh Calvinistic Melhodiscs.—Betv/em the Methodism of Wales
and that of England there was never any other than incidental
connexion. Indeed, although the name of the Welsh movement
was borrowed from the English, not only was Welsh Methodism
quite independent in its origin, bnt in reality its beginning, as an
evangelical movement, was earlier than that of English Methodism.
From Wesleyan Methodism, fmthermore, Welsh Methodism was
throughout distinguished by the fact that it was Calvinistic in its
doctrine. For some years Whitefield's came was placed by the
leaders of Welsh Methodism at the head of their movement, but
tho connexion was not at any time much more than nominal,
Wiitefield being, indeed, too often and too long together in
America to exercise any real presidency over the Methodism of the
Principality.
Distinction, however, must be made between Welsh Methodism
as an evangelistic movement and as an organization. In its later
aad distinctly organized form, its main elements date from 1811,
while the actual unity and the final consolidation of the organization
date from so recent a period as 1864. At that date we find the
Calvinistic Methodism of North and of South Wales for the first
time united in a common organization and government, and brought
under the supreme control of one "General Assembly."
The spiritual awakening from which Welsh Calvinistic Method-
ism derived its earliest inspiration and impulse began in 1735 and
1736, almost contemporaneously and quite iudependently, in three
different counties of South Wales. Howell Harris, a gentleman of
some position, born and bred at Trevecca in the parish of Talgarth,
couuty of Brecon, is the most prominent name connected with early
Welsh Methodism. His first strong religious convictions and im-
pulses date from 1 735. He was sent to Oxford in the autumn of that
year to " cmo him of his fanaticism," but remained only one term.
On his return to Wales he began to exhort and preach in private
hou.ses and in such buildings as he could obtain the use of, being then
and throughout his life a simple layman. Of learning or theology
he had but little; but he was an extemporary preacher of prodigious
vehemence, and often of overwhelming power and pathos. While
Harris was thus jjreaching in the couuty of Brecon, Daniel Row-
lands had been spiritually awakened at Llangeitho in Cardiganshire,
the two men knowing nothing whatever of each other. Rowlands
was an ordained clergyman, of some learning and of great
Oioquenco. He was a pulpit orator, and carefully prepared his
powerful discourses. In Pembrokeshire, again, in that same year
1735-36, Howell Davies began to preach the same doctrine in the
same spirit as the other two preachers, and with effects scarcely, if
at all, less remarkable. The work thus begun in three distinct
centres within the space of one year was in strict connexion mth
the Established Church, and so continued to be throughout the
l^^t^sitary. These single-mmded preachers pursued their work
in Wales knowing nothing of the parallel work which Whitefield
had just begun in England. In 1738, however, Whitefield, in
the west of England, heard of Howell Harris, and in that year
the two revivalists met in Cardiff. In 1739 Howell Harris had
bemn to extend his preaching tours far and wide, visiting not
only South but North Wales, and, wherever he went, foundin"
religious societies in connexion with the Church of England, of a
character resembling those called Dr Woodward's societies, which
had long been m existence throughout England, the chief difference
being that the Welsh societies were "evangelical," Calvinistic,
and revivalist. It was in the same year that Wesley founded
his society in England. In 1742 the clergymen connected with
193
KmIJ CU™rS^'" °^ '*"" "'"^'^ (Scummical Con/ermce, Weslcyaa Book-
the -nclsh movement were ten in number, and there were labour-
ing in concert with these forty lay "eshoiters," as they wero
called. In that year the hrst ••.association" of Welsh CalWnistio
wl- «^f' ""' '''''*,■'" Watorford or Watford, iu Glamorgnnshire;
that of the AVelsh evangelists. The first Calvinistic Methodist
Conference was bed at \ Vaterrovd, under Whitelield's presidency,
on January 5 1743 eighteen months earlier than AVesley's firat
Conference. For a short time the Calvinistic Melhodisn. of Wales
was linked to that of England. Alter 174S, however, Whitefield
ceased to act as ,n any sense the oQicial head of the Calviuistio
Methodists of Eng and, and then- orgauizatiou, always loose, was
gradually dissolved.
There was no Wesley in Welsh Methodism, and aciordin''ly there
was no organic unity among the societies of earlier Welsh Tllethod-
ism. Each local society was under the care of an •'cxhortcr " au
unpaid layman. A number of these local societies were "rouued
together into a district, over which an "overseer" had chan-e He
also was usually an unpaid layman, although excreisiu" many of
the functions of a spiritual pastor. Sometimes, howcvc " a'; in the
case of Rowla.ids, he was a parish clergyyian. The societies
attended their parish cluirchcs and there received the sacraments.
The meeting- or preacliing-houscs for the societies were vaguely
called •'houses for religious purposes."
In 1751 Howell Harris ceased to iriuerate and retired to Trevecca.'-
From this time his leadership in the Methodist movement seems to'
have come to an end, and the movement languished for many years
after. Not till 1762 is any " revival " chronicled. In 1703 Row-
kndswas obliged to quit his cuiacy at Llangeitho ami leave tha
I Established Church. His people built him a chapel. Ho thas, after
1763, became a Dissenting mmister ; and, retaining his fame and
much of his power to the end of his comse, he died in 1790.
Fifty years had now passed since the firet societies of Welsh
Methodism had been established by Howell Harris, ami the move-
ment, instead of having grown to strength au<l maturity, ajipcared
to have spent its force, almost iu all directions, at least so far as
any outward signs could show. But the Rev. Thomas diaries
of Bala was to be one of the chief means of reviving it. He, hke
the earKer Methodists, was a chnrchuiau; he had taken his d'crce
at Oxford and served a curacy in Soinei-setshire. The doors ol°tlio
Established Chmch having been closed against him because of his
style of preaching, he joined the Welsh Jlethodists in 1786, and
his first sphere of marked influence was in North Wales. In 1791
he took a leading part in a great revival of which Bala was the
centre. From this period may be dated the second spriug of Welsh
Calvinistic Methodism, from which its later successes were to gi-ow.
Charles zealously and successfully promoted the establishment of
"circulating schools" and of Sabbath schools. Ho was, iu fact,
the soul of the great Christian educating movement in Wales which
began in the last decade of the IStli century; and it was through
his earnest zeal iu seeking to provide Bibles for his Welsh schools,
especially the Sunday schools, that the British and Foreign Bible
Society was established. Though Methodism came then to be
elfectuaUy rooted in the soil of the Principality, it was not till
1811 that the Welsh Calvinists took that step in the direction of
ecclesiastical independence which the English Wesleyaus had taken
sixteen years before by calling their preachers to the oHicial position
of pastors and ordaining them to administer the sacraments.
From 1790 till almost the present tmic the work of gradually
moulding the constitution of^ Welsh Calviuistio Methodism has
proceeded. The "rules regarding the proper mode of conducting
the quarterly association " were drawn up by Charles and a''rccd
upon in 1790. In 1801 the Order and Form of Church Govcrnvient
and Rules of Discipline wero published. In 1811, as has been
shown, ministerial ordination was initiated. In 1823 the Con-
fession of Faith was promulgated. And iu 1864, as has been
already mentioned, the first "General Assembly "was held, and
the two associations of North and South Wales respectively were
united into one body. The constitution is now a modifieil Prcs-
byterianism, each church managing its own affairs subject to
successive appeal to the monthly meeting of the county and the
quarterly association of the province, while the latter body may
refer the decision to the annual General Assembly.
The Welsh Methodists (or Welsh Presbyterians, as they are
now often called) have two theological colleges, one at Bala and
the other at Trevecca. They have also a foreign missionary society,
with missions in Brittany, among their congeners of the Celtic
race, and in Bengal.
In recent years this church has made great progress. In 1850 the
number of members was 58,678, in 1870 it was 92,735, and in 1880
the returns showed 1174 churches, 118,979 communicants, 185,635
Sunday scholars. The number of ministers is not ofiicially given,
but is estimated at 600. The North and South Wales associations
are now also known as synods.^ (J. H. RI.)
•■' See W. Williams, WtUh Calrtni.
and Timei o/ Hoteetl Harris ; Tycl
Diary of the Calviitlnic Melluxlisls, I882!
XVI. — 25-
194
M E T — M E T
METHODIUS, the apostle of the Slavs, was a native
of Thessalonica, and was born about the year 825. His
nationality is unknown, but most probably he was a
GrscLsed Slav; the family of which he was a member
appears to have been one of considerable social distinction,
and ho himself had already attained high ofEcial rank in
tie government of Macedonia before he determined to
abandon his secular career and embrace the monastic life.
His younger brother Constantino (better known as Cyril,
the name he adopted at Rome shortly before his death)
had also distinguished himself as a secular " philosopher "
in Constantinople before he withdrew to the cloister and
to solitude. Constantino about 860 had been sent by the
emperor Michael III. to the Khazars, in response to their
request for a Christian teacher, but had not remained long
among them ; after his return to within the limits of the
empire, his brother and he laboured for the instruction of
the Slavonic or Slavonici^ed population, especially by
means of translations of the Scripture lessons and the
liturgical books used in Christian worship. About the
year 863, at the invitation of Rastislav, king of " Great
Moravia," who desired the Christianization of his subjects,
but at the same time that they should be independent of
the Germans, the two brothers went to hia capital (its site
is unknown), and, besides establishing a seminary for the
education of priests, successfully occupied themselves in
preaching in the vernacular and in diffusing their reUgious
literature. After four years they seem to have received
and accepted an invitation to Rome from Pope Nicholas
L, who had just been eng3,ged in. his stUl extant corre-
spondence with the newly converted Bulgarian king ; his
death occurred before their arrival, but they were kindly
received by his successor Hadrian 11. Constantiae died
in Rome, but Methodius, after satisfying the pope of his
orthodoxy and obedience, went back to his labours in
"Moravia" as archbishop of Parmonia. His province
appears to have been, roughly speaking, co-extensive with
the basins of the Raab, Drave, and Save, and thus to have
included parts of what had previously belonged to the pro-
vinces of Salzburg and Passau. In 87 1 complaints on this
accoimt were made at Rome, nominally on behalf of the
archbishop of Sabburg, but really in the interests of
the German king and his Germanizing ally Swatopluk,
Eastislav's successor; they were not, however, immediately
successful. In 879, however, Methodius was again sum-
moned to Rome by Pope John VIII., after having declined
to give up the practice of celebrating mass in tho Slavonic
tongue ; but, owing to the pecidiar delicacy of the relations
of Rome with Constantinople, and with the young church
of Bulgaria, the pope, contrary to aU expectation, ulti-
mately decided in favour of a Slavonic hturgy, and sent
Methodius (880) back to his diocese with a suffragan
bishop, and with a letter of recommendation to Swatopluk.
This suffragan, a German named Wiching, unfortunately
proved quite the reverse of helpful to his metropolitan,
and through llis agency, especially after the death of John
VUI. in 882, the closing years of the life of Methodius
were embittered by continual ecclesiastical disputes, in the
course of which ho is said to have laid Swatopluk and his
supporters under tho ban, and the reahn under interdict.
The date of the death of Methodius is variouiily given ;
the most trustworthy tradition says that it took pLace on
April 6, 885. He was buried at Wclehrad (probably
Stuhlweissenberg). The Greek Church commemorates St
Cyril on February 1 4 and St Methodius on May 11 ; in
the Roman Church both are commemorated on March 9.
Seo Schafarik's Staioisckc AlUrthumcy^ whcro tho original
authorities are fully referred to. Tho subject of the present notice
is most probably not to bo identified "with tho Methodius, a painter
and monk, who, according to a well-known legend, converted Boris
'Of Bulgaria by means of a picture of Clirisf a second coming.
METHYL, a chemical term which until lately was used
in two radically different senses, namely, as designating
either the atom-group CHj, which in numberless chemica!
formulae figures as a " radical " (compare Chemistey, vol.
V. p. 552), or a gaseous substance of the same composition,
which, however, nowadays is generally called " dimethyl,'
to distinguish it from the radical A gas of the composi-
tion and the specific gravity (CoH^ -^ Hj = 1 5) corresponding
to C.,H(j can be produced in two principal ways,— first,
by the decomposition of zinc-ethyl by water (Frankland) —
ZnCC2Hj)3-h20H . H = Zn(OH)j -I- CjHjH ;
and, secondly, by the electrolysis of acetate of potash
solution (Koibe), we have virtually
2CH3 . COOH = (CHaX, + 2CO2 1 •)- H, .
-fpole. I —pole.
These two gases used to be distinguished as two different
substances, — Frankland's being looked upon as hydride of
ethyl, C2H5 . E, Kolbo's as " real methyl " (CH3)(CH3)|
imtU Schorlemmer proved their identity by showing that
both, when treated with chlorine, yield the same identical
chloride of elhyl, C2H5 . CL This confirmed the now
generally a<io])ted notion that the radical ethyl itself is
nothing but methylo-methyl, H3C — CH.,*, so that the
filling up of the gap* by an H must necessarily produce
" hydride of ethyl " and " dimethyl " va one. The " true
methyl " which ■;hemists used to dream of, and which, when
treated with chlorine, would yield two CHjCl's analogous
to HH -t- ClCl = HCl + HCl, does not, and according to our
present knowledge cannot, exist. A quasi apology for it is
"marsh gas," (^H^, tho principal component of the gas
mixture which 1 lubbles up from any marshy pond when its
mud is stirred up with a stick. It is always produced
when vegetable matter decays in the presence of water,
and in the relative or absolute absence of air. What
everybody known as " fire-damp " is nothing but a (neces-
sarily explosive) mixture of air with impure marsh gas,
produced in the constantly ;)rogressiug metamorphosis of
the coal deposit? ; in certain districts streams of marsh gas
are issuing forth from cracks in the earth ; the " holy fire "
of Baku is sucii a marsh-gas spring, which, having once
caught fire by accident, continues burning to this day.
Perfectly pure marsh gas can only be obtained from ziac-
inethyl, Zn(CH<)2, by its decomposition with water (vide
supra) ; a nearly pure preparation is procurable by heating
a mixture of acetate of potash or soda and caustic alkali to
dull redness : —
Marsh gas can be prepared synthetically by the action
of bisulphide of carbon vapour and sulphuretted hydrogen
(both producible from their elements) on red-hot copper,
CS, -f 2H2S -1- 8Cu = 4CuoS -I- CHj (Bcrthelot). A mixture
of marsh gas and chlorine, when exposed to direct sunlight,
explodes with formation of hydrochloric acid and char-
coal In diffuse dayhght only part of the hydrogen is
eliminated and " replaced " by its equivalent in chlorine,
which in general leads to the formation of four bodies :
CH3Cl = CH,-)-Cl.,-HCl, chloride of methyl ; CH^Clj,
chloride of methylene ; CHCI3, chloroform ; CCl,, tetra-
chloride of carbon. Of these several chloromethanes, aa
they are called!, tho first here interests us more than any
of the rest, because from it any other methyl compound
can be produced by the substitution of the proper kind of
radical for the CI of tho CH^CL Thus, for instance, we
can convert it into methyl-alcohol by treating the chloride
with aqueous caustic potash at 100° C. (Bcrthelot). This
is a most important synthesis, because it is this methyl-
alcohol that, in practice, always serves as the starting
point in the preparation of other metliyl compounds
Methyl- Akohol. — This substance, in ordinary practice,
METHYL
195
is never made synthetically, bnt simply extracted from
wcxxl-spirit, a commercial substance which is produced
industrially in the dry distillation of wood. The wood-
spirit is contained in the_ aqueous portion of the tar pro-
duced in this operation, along with acetic acid. To recover
both, the tar-water is neutralized with lime and distilled,
when the acetate remains, while the spirit distils oyer,
along with a deal of water, which, however, is easily
removed, as far as necessary, by redistillation and rejection
of the less volatile parts. The "crude" wood-spirit, as
thus obtained, is not unlike in its general properties to
ordinary spirit of wine, from which, however, it is easily
distinguished by its abominable smell. The ordinary
commercial article, besides a variable percentage of water,
contains from 35 to 80 per cent of methyl-alcohol ; the
rest consists chiefly of acetone, but besides includes
dimethyl-acetal, C2H^(OCH3)2, acetate of methyl, and
numerous other minor components. In Great Britain
large quantities of wood-spirit are used for the making
of methylated spirit, a mixture of ordinary spirit of wine
with one-ninth of its volume of wood-spirit, which is
allowed to be sold duty free for the preparation of
varnishes, and for other industrial purposes. In former
times, here as elsewhere, wood-spirit itself used to be
employed as a cheap substitute for spiritus vini ; but this
is no longer so, since the aniline-colour industry has created
a large demand for pure methyl-alcohol. Hence in some
Continental works the wood-spirit, instead of being sent
out as such, is being worked up for its components, by the
following sequence of operations : — (I) dehydration by
lime ; (2) heating, under an inverted condenser, with
caustic soda, to convert the acetate into hydrate of methyl ;
(3) destruction of the bad smells by mild oxidation ; (4)
distillation in a kind of Coffey's still, whereby it is split
up into approximately pure alcohol, acetone, and " tails."
The new industry led to the invention of the following technical
methods for the determination, in a given spirit, of the percentages
of real methyl-alcohol and of acetone.
The alcohol ia determined by saturating 5 c.c. of the spirit with
hydriodic acid (volatilization of alcohol and iodide of mctnyl being
avoided by means of a cold-water bath and an inverted condenser),
and the product poured into water. Iodide of methyl separates
out as a heavy oil, which is measured as it is. According to direct
trials 5 c.c. of pure methyl-alcohol yields 7'45 c.c of crude iodide
(Krell, Kramer and Grodzky).
For the determination of the acetone the following reagents are
required (Kramer) :■ — (1) a solution of iodine, prepared by dissolv-
ing l2=^254 grammes of iodine, by means of (say) 500 grnramea
of iodide of potassium, in water, and diluting to 1 litre ; (2) a
solution of caustic soda containing twice (NaOH) grammes per litre ;
(3) alcohol-free ether. Ten c.c. of the soda are placed in a gra-
duated cylinder and mixed intimately, first with 1 c.c. of the spirit,
then with 5 c.c. of the iodine solution. Iodoform separates out (if
acetone is present) in minute yellow crystal plates ; this product is
•'shaken out" by means of 10 c.c. of ether, and determined by
evaporating an aliquot part of the ethereal layer in a tared watch-
flass to dryness and weighing the residue. C3HJO yields CHI3;
ence 1 part of iodoform indicates 0'28 parts of acetone.
The formula of methyl-alcohol and its true chemical
character were correctly ascertained by Dumas and P^ligot
as early as 1834 ; yet pure methyl-alcohol may be said to
have been an unknown substance until 1852, when Wohler
taught us to prepare it, by first extracting the CH, of the
CH3OH in the wood-spirit as oxalate of methyl, and then
decomposing the (purified) oxalate with water.
The most convenient raw material to use nowadays is the
commercial *' pure " alcohol ; if wood-spirit is employed it had
better first be purified by distillation over caustic soda {vide sitpra).
The formation of the oxalate then is best effected (according to
Alexander Watt) as follows : — 500 grammes of oxalic acid crystals
are mixed with 200 c.c. of oil of vitriol ; then 500 c.c. of the
npirit are added, the whole kept for a time at 80° C, and thou
allowed to stand cold for twenty-fonr hours.
The lane crop of oxalate crystals— partly (CK3)jC.0t, partly
CU|. H . CtO^ — IS separated from the liquor by pressure sod subse-
quent drjing over vitriol, and then decomposed by distillation with
water.
The nqueons alcohol thus olit;iincd is dolivdr.ilcil by the well-'
known methods used iu the prepanilimi of onliiKiry iib-iolule nlcoliol.
According to Kiauior, a purer prciiaratioii tli.in \V,.lili'i'a is
obtaiued by extracting the nieth) 1 as foriiiiali.' in»lc:id of as o.\:ilate,
which is easily cli'ci-lJa by digesting tlio wood-spirit wiili a I'oriiiio
acid of 122 specific gravity, and mirifying the fovmic etlicr by
fractional distilUtion. Tliis ctha' boils at Si", the o.vahitr at Ifil'
C, hence a proper conibiuatiou of the two nirthods should bo
infinitely supci ior to citlier. What now follows must, in general, be
uudei-stood to refer to Wiihler's preparation.
Pure methyl-alcohol is a colourless liquid similar in its
general properties, in its behaviour to other chemically
inert liquids, and in its action as a solvent to ordinary
absolute alcohol, from which, however, it differs by the
entire absence from it of all sjiirituous odour. A pre-
paration which smells of wood-s])irit may bo condemned
at once as impure. According to H. Kopp, ita sjjecific
gravity is 08142 at 0° C. and 07997 at 16''-4. If the
volume at t° be V, then (from 0° to 61°)
V = l■^••OO0n3«-l-l■364xlO-V-^8•741xlO-V.
The boiling point is 64°-6 to 65°2. The tension-curve was
determined by Eegnault and by Landolt ; but the results
of the two observers do not agree except (approximately)
at P = 760 mm.. Jlethjl-alcohol has quite a characteristic
tendency to " bump " badly on distillation, which, however,
can be prevented by addition of a small fragment of tin-
sodium, which produces a feeble but sufficient current of
hydrogen. Itsspecificheat is "0713 ; latent heat of vapour,
26"4 ; combustion heat, 5307 per unit weight fFavie and
Silbermann). The refractive index for the D (sodium)
ray is I -3379. ± -0013 for 10° =? 5° C. (Dale and Gladstone):^
Methyl-alcohol mixes with water in all proportions with
contraction.
Since Wohler's discovery a table for the specific gravities of
aqueous methyl-alcohols has been constructed experimentally by
A. Dupr^ ; but unfortunately his alcohol boiled at 58'7, and con-
sequently must have been something dilTereut from what gcnci'ally
goes by this name.
In its chemical reactions methyl-alcohol, CH3 . OH^ is
very similar to ordinary (ethyl) alcohol, CjH^ . OH, and
consequently, in the same sense as the latter, analogous to
water, H.OH. Thus, for instance, metallic sodium and
potassium dissolve iu either alcohol with evolution of
hydrogen and formation of ethylatcs or methylates of the
alkali metals. Example —
CHjOH-t-Na = CH3. OJfa+JHj.
The two methylates crystallize from the solution with
crystal-alcohol, which can be driven off in an atmosphere
of hydrogen by heat, without decomposition of the salts
themselves. Water at once decomposes them into caustic
alkaU and alcohol, CHj . ONa -1- H . OH = NaOH + CH3OH.
Yet the reverse reaction takes place when the alcohol is
treated with a large excess of caustic soda.
The action of acids on methyl-alcohol is in general
quite analogous to that on, for instance, cau'stic soda, with
tills important difference, however, that what in the caso
of NaHO goes on so readily in aqueous solutions with
CH3 . OH succeeds only under circumstances precluding
the accumulation of water. In these circumstances wa
have, for instance,
(1) CIH -H OH . CH,=H,0 ■^ CI . CH3 ;
and so on with all monobasic acidc, A dibasic acid XHH
may act as {X)R, or as (XH) . H ; thus, for instance,
(3) (CjO^H)H + OH.CH3=H20 + CjO..HCR, ;
Oxalic acid. lletliyl oxulic add.
(4) (C,0,)H,-|-20H. CH,-2HjO-fCjO,. (CUj),i
Methyl oialate.
196
M ETHYL
A tribasic acid forms two methyl acids and one neutral
ether ; we have, for instance,
(j) (From I'OjH.,,; I'OjfCHj; II, ; rOj(CH,)jH ; P04(CH3)j.
It ivouM, however, be a great mistake to suppose that
whether, for instance (Ex. 3 and 4^, the mononiethyl or
the dimethyl compound is formed depends on the quantity
of methyl-alcohol employed per unit of acid. This depends
far more largely on other conditions, as will be illustrated
ill next paragraph. The methyl-salts of oxygen acids are
called esters, in oiiposition to the chloride, bromide, iodide,
sulphide, and oxide, which are set apart as ethers. Broadly
sijcaking, ethers are not, while esters are, readily decom-
]io.ied by water into their cogeners ; but the nitrate
C'Hj . XOj behaves in this respect like an ether.
ArUonwiih Sulphuric Acid. — Methyl-alcohol mixes 'with
oil of vitriol with considerable evolution of heat and (always
only partial) conversion of the two ingredients into uicthyl-
sulphuric acid. Ecjual volumes of acid and alcohol give
a good yield. To prepare pure methyl sulphates, dilute
the mixture largely with water, avoiding elevation of
temperature (which would regenerate the ingredients), and
saturate with carbonate of baryta. Filter off the suli)hate
of baryta to obtain a solution of the pure methyl sulphate
bOj . CHj . ba (where ba = iBa = 1 c/.), from which this
salt is easily obtained in crystals. From the baryta salt
any other methyl .sulphate is readily obtained by double
decomposition with a solution of the resjicctive sulphate ;
the acid itself, for in.^tance, by means of sulphuric acid.
At higher temperatures the reaction between vitriol and
methyl-alcohol results in the formation of methyl-ether,
(CH.|).,0, or of normal sulphate of methyl, (CH3).,S0.,.
The ether is a gas condensable into a liquid which, under
pressure of one atmosjihere, boils at- 21° C.
The gas dissolves in about one thirty-seventh of its volume of
water ; tar more largely in alcohol and in ether; most abundantly
in oil of vitriol, which dissolves about six hundicd times its
volume of methyl-other gas, thus alTurding a very liandy means
for storing up the gas for use. The solution needs only be diluted
with its own volume of water to be broken up into its components
(Eilcnmeycr).
Liquefied oxide of methyl is now being produced on the
manufacturing scale, and sold as a powerful refrigerating
agent. One part of sulphuric acid is mixed with a little
over one part of dehydrated wood-spirit, and the mixture
heated to 125° to 128' C. (130° being carefully avoided),
when methyl-ether goes off. When the mixture is
exhausted, more wood-spirit is added to the residue so as
to re-establish the original specific gravity (of 1'29), and
the heating resumed, which again furnishes a supply of
the gas, and so on. This ])roves that the process is not, as
used to be supposed, one of mere dehydration, but a cycle
of reactions analogous to those in the ordinary process of
ctherification, as shown by the equations : —
(1) S0jH;-^CH30n = S0j. HCH3+H,,0.
(2) &O4. il. Cllj-H H. 0. CHj-SOjHH-l-CHa.O.CHj.
Th.- ester, SO^iCir,), though obtainable by distillation of the
aleohol willi in parts of vitriol, is more couvenientlv prepared IVoni
pure niethvl-sulplmrio acid hv dislillntion in vucuiiin at 130°-HO'
C; llius:--2SiljCll.,. H-SOjII.,.hSOj(CH,,V.. It is a colomlcss
li.|uiil, sniclliiig like peppermint, spceiUe gravity 1-327 at 18°; it
boils at 187' to 188° C.
Chloride o/mdliyJ, CHjCl, readily produced by the action
of hydrochloric acid gas and hot methyl-alcohol (preferably
in the presence of chloride of zinc as an auxiliary dchy-
drator), is a gas which, under ordinary pressure, condenses
into a liquid at - 23' C. The gaS, at ordinary temperatures
(though very readily soluble in alcohol), is only sparingly
absorbed by water, which, however, at 6° unites with it
into a solid hydrate. Condensed methyl chloride ha.<!
Ijecoine an article of commerce, being largely produced
frora.trimethyiamine (vidn iii/ra) and used aa a powerful
j frigorific agent, as well as for the cxtra'ition of peffiinlM
from flowers. Regarding nitrite of methyl, NO — O — CHj,
its interesting isomeride uitromethane, O.^N — CH^, and
I nitrate of methyl, N0.,CH3, we must refer to the hand-
j books of organic chemistry.
Iodide of methyl, CH3, is obtained by distilling methyl-
j alcohol with hydriodic acid, which latter is best produced
. off-hand by addition to the alcohol of iodine and amorphous
phosphorus. It is a colourless liquid of 2'269 specific
gravity, boiling at 42°'5 C, insoluble in water.
Ori/anir Melhyl- Esters. — The more volatile ones are in
general easily obtained by distillation of the respective
arid with methyl-alcohol, or with methyl-alcohol and oil
of vitriol (virtually SOj . H . CH^) ; the le.5s volatile
ones more conveniently by passing hydrochloric acid gaa
into a methyl-alcoholic solution of the acid. We have no
space for the individual substances ; but the salicylate
CjHjOj . CH, may just be named as being the principal
component of the essential oil of Gaull/uria procumbent
(wint'ergreen oil).
Methylamines. — The general result of the action of
ammonia on an ester is the formation of alcohol and acid
amide. Example —
CaHjO)- 0-CH3 + HNHj = CH3 . OH-hCoHjO. NH..
Acetate oi rautliyL AcelaiiilJc.
With iodide of methyl this reaction is an obvious im-
possibility ; what really takes place (as A. W. Hof mann
has shown for this and all analogous cases) is that the
iodide unites with the ammonia into the HI compound
HI. NHiCH, of a base NUjCHj, which can be separated
from the acid by distillation with caustic ijotash, and when
thus liberated presents itself as a gas surprisingly similar
(almost to identity) to ammonia. The analogy extends to
the action on iodide of methyl, which, in the case of methyl-
aniine, NH.CHj, leads to the formation of diniethylamine,
NH.(CH3)^; and from the latter again trimethylamine,
N(CH3)3, can be prepared by a simple repetition of the
operation. These three amines are closely analogous in
their chemical character to ammonia, the points of differ-'
ence becoming the more marked the greater the number of
(CH3)'s in the molecule. Trimethylamine, having lost all
its ammonia-hydrogen, cannot possibly act upon iodide of
methyl like its analogues. What it really does is to unite
with the iodide into "iodide of tetrametliyl-ammonium,"
I . N(CH3)j, analogous to iodide of ammonium, INHj, we
should say, if it were not the reverse, because the organic
■ iodide (unlike its prototype, which is an ammonium
j compound only in theory), when treated with moist oxide
I of silver (virtually with AgOH), really docs yield a solution
of a true analogue of caustic i)otash in the shape of
' hydroxide of tetramethyl-ammouium, N(CH3)j. OH.
In regard to the actual preparation of .these several
I bodies, which is not so simple as might appear from our
I exposition of their mutual relations, we must refer to the
j handbooks of organic chemistry. But we must not omit
'1 to state that trimethylamine, which only the other day
was never seen outside a chemical museum, is now being
manufactured on a large scale, and promises to play an
1 important part in industrial chemistry. The waste liquors
' obtained in the distillation of alcohol from fermented bectr
I root molasses serve as a raw material for its preparation.
I These liquors, when evaporated to dryness and subjected
I to dry distillation, yield, besides tar and gases, an aqueous
liquid containing large quantities of ammonia, acclonitrile,
methyl-alcohol, and trimethylamine. This liquor is neutral-
' ized with sulphuric acid, and distilled, when the nitrilo
and the methyl-alcohol distil over, to bo recovered by
proper methods. From tlic mixed .solution of the sul[)hatcs
I of ammonia and trimethylamine the former is separated
I out as far as possible by crystallization ; the mother-liquor
METHYL
197
is distilled with lime ; the volatile bases are absorbed in
hydrochloric acid ; the hydrochloric solution is evaporated ;
and the sal-ammoniac which comes out at first is, as far as
possible, fished out. The last mother-liquor is evaporated
to dryness, and in this form represents commercial
trimethylamine hydrochlorate. It is this product which
serves for the preparation of methyl chloride [vide sitpra),
the process being founded upon the fact that a concentrated
solution of the salt, when heated, breaks up 3HC1 . N(CH3)3
into 2N(CH3)3 of free trimethylamine -f NH2 . CH3HCI of
hydrochlorate of monomethylamine and 2CH3CI of methyl
chloride.
These processes are being carried out industriaUy by
Vincent in France. But this base trimethylamine seems
destined to do more than provide us with a new refrigerat-
ing agent. The attempt has been made — it would appear,
with success — to utilize it for the preparation of pure
carbonate of potash from native chloride of potassium,
just as ordinary ammonia, in the famous ammonia-soda
process, serves for the conversion of common salt into soda-
ash.
Methyl Cyanides. — There are two distinct bodies which, by com-
position and by synthesis, are both CH3 + NC; they are named
" acetonitrile " (formerly called simply cyanide of methyl) and
isocyanide of metliyl or methylcarbamine respectively.
Acetouitiile was discovered by Dumas in 1847. It may be pre-
pared by tlie distilhitiou of a mi.\ture of mtthylsulphate and of
cyanide of potassium ; but is obtained more easily and in a purer
Btate by distilling acetamide with phosphoric anhydride. Acetate
of ammonia may be used instead of the amide, but it does not work
BO well
CH,.CO.O(NHJ CH3.C0.(NH.) CH,.CN
Acetate of NH, Acetamide Nitrilo
= A(say). =A-H.O. =A-2HjO.
It is a colourless liquid of a pungent aromatic odour, with specific
gi-avity -805 at 0°, and boils at 82 C. When heated with aqueous
potash (at the wrong end of a condenser) it breaks up with for-
mation of ammonia and acetate of potash. Whence we conclude
that the methyl is combined more directly with the carbon of the
cyanogen, thus :
N { C-CH3} ■(■ 2H.0 = N H3 -H CH, . COOH .
Acetic acid.
This conclusion is supported by the action on the nitrile of nascent
hydrogen, which leads to the formation of ethylamine, thus (Men-
dius) : —
NC— CH3 -HH = H„N— CH2CH3.
Etliyl;itilinc.
In either case we pass from a monocarbon to a dicarbon body,
virtually from methyl to ethyl alcohol.
The isocyanide is prepared by heating iodide of methyl with
ej-anide of silver (CH3I ; 2NCAg) and ether in a scaled-up tube to
^130° to 140", to produce the crystalline body AgNC-hNCCHj (and
Agl). The double cyanide, wlien distilled with some water and
cyanide of potassium, breaks up into its components, — the NC'Ag
forming (NC)j AgK ; and the cyanide of methyl distils over. It is a
colourless liquid, charactenzed by quite an unbearably irritating and
sickening smell. The specific giavity is 756 at 14°, the boiling point
£9° C. It combines with hydrochloric acid into a crystalline salt
vhich is readilydecomposed by water into methylamine and formic
acid. Whence wo conclude that in this case the cyanogen is tied
to the methyl by its nilrog-^n ; thus :—
C{N-ClIj}+2H,0 = Il.C00H-hNH...CH,.
Fonnlc aoid, Mc'Ii^-liiisine.
The methyl here remains metl^yi, being separated by an N from the
cyanogen-carbon, whicU latter passes into fomiic acid.
We must not close this section without at least referring to
the me'.Ii'jipkosphincs, as being a set of bodies related to PH,
(phosiiiune)asthemetliylamincsare to NH, (.immonia), and similar
tj> "liese in their chemical character, in so far as they are bases.
Ae points of difference between the two scries are of pretty much
in-5 same sense as those between the two prototyjics. Thus, for
Aiitance, while trimethylamine NlCHa)^ is a strong base, but inert
■o oxygen gas, trimcthylphosphine k a lelativcly feeble base,
oiit in contact with air greedily absorbs o.vygen with formation of
e.i^oxide JP(CH3)30, the like of which in the nitrogen series has no
existenop.
S'!(/pfiirCOTn;)fli(iirf.«<)/i/c%Z.— Substances analogous to methyl-
alcohol and methvl-cther respectively can be obtained by the dis-
tillation of methyl sulidiatc of jiotassium with) strong solutions of
the p^assmm sulphides EH6 and KjS respectively. The body
CHj.bH IS known as melhyl.mercaptaue, tlio other (CH,).,S aa
sulphide of methyl. Both are very volatile stinking li.mids.
Sulphide of methyl claims a special interest as being the starting
point for the preparation of an important class o( boilics callcS
trymethyl su phine coirpouuds. The sulphide ((. ll,).,S readily
unites Kith the iodide CH,,I into crystals of iodide of'trimethyl
sulphine, (CH3)3S. I, a substance which is closely analogous in its
chemical character to the iodide of tctiamctli.\ 1-ainiiiouiimi Hoist
oxide of silver, for instance, converts it into a "stronyly bisic hydrate,
S(CH3)3 • OH, which m its avidity for acids almost bents its analo-'ou
in the nitrogen family. An investigation of its salts w.as published
by Crum Brown and Blaikie.
McUiJjl ^)sciiiifc5.— Ai-scuiferous bases constituted like mono- or
ui-methylamine (bodies such as AsHXHj, aniilogous to KH„. CH.)
do not seem to e.\ist What we do "know of are— (1) a triuielhyl-
arsine and the iodide and the hydroxide of tctranietliyhu sonium
— As(CH3)3, As(CH3)jI, and As(CH3),0H,— bodies discovered by
Cahours and Riche ; (>) a whole series of monomctliylic bodies
As(CHa)X2 (where X = C1, Br, orXj-O.S), discovered by Raeyeriii
18.57 ; (3) the kakoJyle compouuds, a series of boilies, As(Cii3)., . X
or As(CH3)o. Xj, which were discovered and iuvestigatcd by li. Bunseii
in 1842. This great investigation marks an epocli in the history of
organic chemistry, and our article would not be complete without at
least a short summary of ite results. Bunseu started in his investiga-
tion with a liquid which had been obtained by Cadet .as early as 1 7ijO,
I by the dry distillation of equal parU of white ai-scnic and anhydrous
acetate of potash, and which nobody cared to investigate because
it emits fumes which have an indescribably sidieniiig smell and an
intensity of poisonous action, compared with which that of white
arsenic itself appears insignificant. It was rcseived for Eunsoii to
attack this awful substance and force it to give an account of if self.
According to Bunsen, Cadet's liquid is substantially an oxide,
(AsCoHjUO, which has strongly basic properlics, readily exchang-
ing its O forClj, &c. To obtain the pure substance, tl.c liquor is
distilled with corrosive sublimate and hydrochloric add, which in
the first instance yields the pure muriate of the base As(Cll ,)..C1,
in the form of a liquid volatile above 10U° into vapours which take
fire spontaneously in air. Fiom this chloride of kakodyht the pure
oxide is obtained by distillation Avith caustic potash. The pure
o.xido emits no fumes; its specific giavity is 1-462; it boils near
150°. A mixture of its vapour with air detonates at 50° C. From
the chloride again, Bunsen obtained the fice radical lakodyU,
(AsCiH,,);, by treatment with metallic zinc iu a special apparatus,
so constructed that all the several operations involved could be
carried out without bringing the contents iu contact with air,^'
a necessary precaution, because kakodyle is a liquid which takes
fire in air spontaneously even at ordinaiy tcmiieratures. Pure
kakodyle is a heavy colourless liquid boiling at about 170° C, and
freezing at -6°. When exposed to o.vygen or chlorine it sull'ers
destructive combustion ; but on slow access of air it is oxidized into
its oxide, (AsCjHJ.O, and kakodylic acid; with chlorine water it
unites into the chloride whidi it came from ; it also unites directly
with sulphur and other olemeiiti ; iu short, it is exactly to kako-
dyle compounds what potassium is to potash and potash salts,
"a true organic element," as Bunsen himself put it. 'J'liis dis-
covery of Bunsen's was greeted with an enthusiasm which it is
difficult in these days to realize. Witli us now, a radic:d is
intrinsically a fiction ; it was dilferent in 1842. By the isolalioii
of kakodyle the "radical" notion suddenly rose from an unproved
hypothesis to the rank of a theory based oil expeiinient. Still,
however much our theoretical uotions may shift, Buusou's lesear.-'*
will stand as a piece of monumental scientific worl^
Kakodylic acid, As. O. (CHj),. OH. i= .-,i.-<:t .'=i--^-.;;1^.-;l!y pre-
pared from the oxide by addition of watif .-.r.d ov.\\s of mercury,
H„0-H2HgO supplyiugthc H.-i-O, re<;:;:rt:.-i :orl(AsCHr.)jO. This
is a crystalline monobasic aci-J, aoiuble in water. " Unlike the
kakods'lides of the As. S3 type, it has no smell, and is no very
violent poison, it takes six grains of it to kill a i-abbit.
Mtlrxllic ilcOi itifts.— Examples of these are— Sb(CH3)3 j SWCIU). ;
JIg(CH3). ; Zn(CH3)2 ; PMCHs)^; AHCHj),, ; SiKCllj)^ . To give an
idea of the chemical character of this interesting class of bodies we
choose zi/ic-iiuthyl as a representative examide, and state briefly
the chief points of its chemical history. This body was discovered by
Fiankland in 1849. It is prepared by boiling iodide of methyl over
granulated zinc in a flask connected with an uiverted condenser, and
so contrived otherwise that the contents are protected against access
of moisture and oxygen. Under these circunislances the two in-
fredients gradually unite into a non-volatile and solid eoinpoiiud
Zn.(CH3). When this body is heated with more of iotlide of
methyl, it undergoes dctfoniposition, with fomiation of iodide of
zinc and of dimethyl gas, I— Zn— CH3 + CHsl-Znlj-KCll3)3,
which reaction to some extent takes place unavoidably in the pre-
paration of the zinc salt, however great an excess of metal may bo '
taken. What survives needs only to be subjected to dry distillation
(iu the absence of air) to yield a distillate of zinc-methyl: —
2I_Zn— CH8=.ZnIj-l- Zu(CH3)j,
19«
M E T — M E T
Zinc-methyl is a colourless liquid of 1 'SSS spccifvc gravity at 1 0°-5,
which boils at 46° Ci in contact with air it takes lire. Water
dccniniioses it at once into hydrate of oxide of zinc and marsh gas,
Zii(CH3), = Zn(OH)j + 2CH3H. Of other reactions the following
may lie named. (1) When digested with sodium, it yields a prccipi-
^t-ite of metallic zinc, and a double compound of itself and sodiura-
Vncthyl. This latter unites readily with carbonic acid into acetate
of .soda, ^■aCH,^-C0J=.C■H3— CO— OXa (Wanklyn). (2) With
chloride of acetyl it forms' acetone, Zn(CH3)j + 2CH, . CO . CI =
ZnClj + 2CO(Cll3)j(FreunJ). (3) Under somewhat different condi-
Tions, includiii;^ the presence of an excess of Zn(Cf-^.^),_,, a compound
is produced which with water, yields tertiary butyl-alcohol (Boutle-
row) :*
COtCHj)^ + Zn(C Hj), - C(CH3)3 . 0 . ZnCHj = A ; ,
A+2H.0H =Zn{0H)j + CH, + C(CH»)3-0H.'
Tertiary alcoliol. (yf^ D. )
METRONOME, an instrument for denoting the speed
at which a musical composition is to be performed. Its
invention is generally, but falsely, ascribed to Johann
Nepomuk MaeUel, a native of Eatisbon (1772-1838). It
consists of a pendulum swung on a pivot; below the pivot
is a fixed weight, and above it is a sliding weight that
regulates the velocity of the oscillations by the greater or less
'distance from the pivot to which it is adjusted. The silent
metronome is impelled by the touch, and ceases to beat
when this impulse dies ; it has a scale of numbers marked
on the pendulum, and the upper part of the sliding weight
is placed under that number which is to indicate the
quickness of a stated note, as M.M. (Maelzel's Metronome)
<:)= 60, or « = 72, or • = 108, or the like. The number 60
implies a second of time for each single oscillation of the
pendulum, — numbers lower than this denoting slower, and
higher numbers quicker beats. The scale at first ex-
tended from 50 to 160, but now ranges from 40 to 208.
A more complicated metronome is impelled" by clock-work,
makes a ticking sound at each beat, and continues its action
till the works run down ; a still more intricate machine
Las also a bell which is struck at the first of any number
of beats willed by the person who regulates it, and so
signifies the accent as well as the time.
The earliest instrument of the kind, a weighted pendidum
of variable length, is described in a paper by litienne Loulii
(Paris, 1696; Am.sterdam, 1698). Attempts were also
made by Enbrayg (1732) and Gabory (1771). Harrison,
who "ained the prize awarded by the English Government
for his chronometer, published a description of an instru-
ment for the purpose in 1775. Davaux (1784), Pelletier,
Abel Burja (1790), and Weiske (also 1790) described
their various experiments for measuring musical time. In
1813 Gottfried Weber, the composer, theorist, and essayist,
proposed a weighted ribbon graduated by inches or smaller
divisions, which might be held or otherwise fixed at any
desired length, and would infallibly oscillate at the si\me
speed so long as the impulse lasted ; this, the simplest, is
also the surest, the most enduring, the most portable, and
the cheapest invention that has come before the world,
and one can but wonder that it has not been universally
accepted. Stijukel and Zmeskall produced each an instru-
ment ; and Maelzel made some slight modification of that
by the former, about the end of 1812, which he announced
as a new invention of his own, and exhibited from city to city
on the Continent. It was, as nearly as can be ascertained,
in 1812 that Winkel, a mechanician of Amsterdam, devised
a plan for reducing the inconvenient length of all existing
instruments, on the principle of the double pendulum, rock-
ing on both sides of a centre and balanced by a fixed and a
variable weight. He spent three years in completing it,
and it is described and commended in the Report of the
' ^Nellicrhinds Academy of Sciences, August 1 4, 1815. Maelzel
thereupon went to Amsterdam', saw Winkel arid inspected
his invention, and, recognizing its great superiority to what
lie called his own, offered to buy all right and title to it.
Winkel refused, and so Maelzei constnictea'a-ebpyot^lBs
instrument, to which he added nothing but the scale -of
numbers, took this copy to Paris, obtained a patent for it,
and in 1816 established there, in his own name, a manu-
factory for metronomes. When the impostor revisited
Amsterdam, the inventor instituted proceedings against
him for his piracy, and the Academy of Sciences decided
in Winkel's favour, declaring that the graduated scale was
the only point in which the instrumen't of Maelzel differed
from his. Maelzel's scale was needlessly and arBitrarily
complicated, proceeding by twos from 40 to 60, by threes
from 60 to 72, by fours from 72 to 120, by sixes from 120
to 144, and by eights from 144 to 208. Dr Crotch con-
structed a time-measurer, and Henry Smart (the violinist,
and father of the composer of the same name) made another
in 1821, both before that received as Maelzel's was known
in England. In 1882 James Mitchell, a Scotsman, made
an ingenious amplification of the Maelzel clock-work,
reducing to mechanical demonstration what formerly rested
wholly on the feeling of the performer. Although
" Maelzel's metronome " has universal acceptance, the silent
metronome and still more Weber's graduated ribbon are
greatly to be preferred, for the clock-work of the other is
liable to be out of order, and needs a nicety of regulation
which is almost impossible ; for instance, when Sir George
Smart had to mark the traditional times of the several
pieces in the Dettingen Te Deum, he tested them by twelve
metronomes, no two of which beat together. The value of
the machine is exaggerated, for no living performer could
execute a piece in unvaried time throughout, and no
student could practise under the tjTanny of its beat ; and
conductors of music, nay, composers themselves, will give
the same piece slightly slower or quicker on different
occasions, according to the circumstances of performance.
METSU, Gabriel, a Dutch painter of celebrity (born
in 1630, died after 1667), is one of the few artists of
renown in Holland whose life has remained obscure.
Houbraken, who eagerly collected anecdotes of painters
in the 18th century, was unable to gather more from the
gossip of his contemporaries than that, as early as 1658,
!Metsu, at the age of forty-three, submitted to a dangerous
surgical operation. The inference drawn by superficial
readers from this statement has been that death immediately
ensued. A more careful pentsal would have shown that
Houbraken knew that Sletsu had given le.ssons to Da
JIusscher in 1665. Local records now reveal that Gabriel
was the son of Jacques Jletsu, who lived most of his days
at Leyden, where he was three times married. The last of
these marriages was celebrated in 1625, and Jacomma
Garnijers, herself the widow of a painter, gave birth to
Gabriel in 1630. Connected by both his parents with art,
Metsu was probably taught first by his father and then by
Gerard Dow. Ho probably finished his training under
Rembrandt. So far back as 1648, but a few days earlier
than Jan Stcen, who is said to have painted his portrait,
Jletsu was registered in the painters' corporation at Leyden;
and the books of the guild also tell us that he remained a
member in 1649. In 1650 he ceased to subscribe, and works
bearing his name and the date of 1653 give countenance to
the belief that he had then settled at Amsterdam, v^tis he
continued his studies under Rembrandt. His companions
at the time would naturally be Do Hooch and Van dcr
Meer, whose example he soon followed when it came to his
turn to select the class of subjects for which his genius
fitted him. Under the influence of Rembrandt he prc>-
duced the Woman Taken in Adultery, a large picture witb
the date of 1653, in the Louvre, in which no one would
suspect the painter of high life or tavcnis were it not that
his name is written at fuU length on the canvas. The
artist who thus repeated the gospel subjects familiar^ta
M E T — M E T
199
Tlinck and Eeckhout was also acquainted with tho Oriental
wardrobe of Rembrandt, and ready to use it, like all his
contemporaries. But he probably observed that sacred
art was ill suited to his temper, or he found the field
too strongly occupied, and happily for himself, as well
as for his admirers, he turned to other subjects for
which he was better fitted. We may doubt whether he
tried the style of allegory as illustrated in a picture of
Justice Protecting Virtue and Chastising Vice in the
gallery of the Hague. There is every reason to think that
this rough and frosty composition was wrought by quite
another master. What Metsu undertook and carried out
from the first with surprising success was the low life of
the market and tavern, contrasted with wonderful versa-
tility by incidents of high .life and the drawing-room.
In each of these spheres he combined humour with expres-
sion, a keen appreciation of nature with feeling, apd breadth
with delicacy of touch, unsurpassed by any of his contem-
poraries. In no single instance do the artistic .lessons of
Rembrandt appear to have been lost upon him. Tho same
principles of light and shade which had marked his school-
-work in the Woman Taken in Adultery were applied to
subjects of quite a different kind. A group in a drawing-
room, a series of groups in the market-place, a single figure
in the gloom of a tavern or parlour, was treated with the
utmost felicity by fit concentration and gradation of
light; a warm flush of tone pervaded every part, and, with
that, the study of texture in stuffs was carried as far as it
had been by Terburg or Dow, if not with the finish or
the brio of De Hooch. Metsu's pictures are all in such
admirable keeping, and so warm and harmonious in his
middle or so cool and harmonious in his closing time,
that they always make a pleasing impression. They are
more subtle in modulation than Dow's, more spirited and
forcible in touch thaij Terburg's ; and, if Terburg may of
right claim to have first painted the true satin robe, he
never painted it more softly or with more judgment as to
colour than Metsu.
That Metsu married and became a citizen of Amsterdam
in 16-59 would only prove that his residence in the com-
mercial capital of the Netherlands was later than historians
have generally assumed. But there is no reason to think
that Metsu claimed his citizenship at once. The privileges
of a burgess were given in exchange for a payment of dues,
and these painters had various ways of avoiding unless they
married. One of the best pictures of Metsu's manhood is
the Market-place of Amsterdam, at the Louvre, respecting
which it is difficult to distribute praise in fair proportions,
80 excellent are the various parts, the characteristic move-
ment and action of the dramatis persotiss, the selection of
faces, the expression and the gesture, and the texture of
ithe things depicted. A tin can in the arm of a cook is a
marvel of imitation, but the cook's face is also a marvel
of expression. Equally fine, though earlier, are the
Sportsman (dated 1661) and the Tavern (also 1661) at the
Hague and Dresden Museiuns, and the Game-Dealer's Shop,
also at Dresden, with the painter's signature and 1662.
Metsu is one of the painters of whose skill Holland still pre-
serves examples, yet whose best pictures are either in England or in
France or in tho galleries of Germany. The value of his works is
large, and at the Pommersfelden sale in 1867 the Jealons Husband
Dictating his Wife's Letters, though hut one of several replicas,
|Was bought by Lord Hertford for little short of £2000, while for
the Ride of the Prince of Orange, in the GkU collection at Vienna,
£3000 was paid by Baron Rothschild in 1878. (J. A. C.)
METTERNICH, Clemens Wenzeslaus, Pkince (1773-
■1859), first minister of Austria from 1809 to 1848, was
the son of a Rhenish nobleman employed in high office by
the Austrian court. He was born at Coblentz in 1773.
'At the age of fifteen he entered the university of Strasburg.
The French Revolution was then beginning. Everywhere
the spirit of hope gave to men's language an exaltation and
a confidence hardly known at any other epoch. But the
darker reality soon came into view. Mettersich was a
witness of the riot in which the town-hall of Strasburg was
pillaged by a drunken mob ; his tutor subsequently became
a member of the revolutionary tribunal in Alsace. If wb
are to trust to Metternich's own account of the formation
of his opinions, the hatred of innovation, which was the'
ruling principle of his later life, arose from his experience,
of the terrible results which followed at this time from the
victory of so-called liberal ideas. But in reality Mettemich
was an aristocrat and a conservative by birth and nature.
His sentiment in things political was that of a member of
a refined and exclusive society which trusts to no intelli-
gence but its own, and hardly sympathizes with larger
interests. The aggressions and violence of the Revolution
from 1789 to 1799 gave Metlernich ag historical basis for
his political theories, but the instinctive preferences of his
own mind were the same from first to last. He began life
as a young man of fashion and gallantry. His marriagd
in 1795 with the Prii^cess Kaunitz, a granddaughter of the
famous minister, fixed iiim in the liighest circle of Austrian'
nobility. His first contact with the great political worli
was at the congress of Rastadt in 1798, where, under the
auspices of the victorious French republic, arrangementsi
vere made for compensating the German princes and nobles
whose possessions on the left bank of the Rhine had been
ceded to France by the peace of Campo Formio. Metternich
was the accredited agent of a group of Westphalian nobles;
his private letters give a vivid picture of the rough and
uncourtly diplomatists who had succeeded to the polished
servants of the old French monarchy. In 1801 Mettemich
was appointed Austrian ambassador at Dresden, and m
1803 he was promoted to Berlin; but he had hardly!
become as yet a prominent man in Europe. His stay af|
Berlin was the turning-point of his life. The war of thej
third coalition was impending. Austria united with England
and Russia against Napoleon, and the task of the youthful
ambassador was to win over the court of Berlin to tho
cause of the allies. Mettermch seems to have done all
that it was possible for him to do ; but Prussia persisted
in its neutrality. The earnestness with which Metternich
had worked against France did . not prevent him from
remaining on the friendliest terms with M. Laforest, the
French ambassador at Berlin ; and so agreeable an account
of him was transmitted to Paris by his rival that, at the
close of the conflict. Napoleon himself requested that.
Mettemich might henceforward represent Austria at the"
Tuileries. Mettemich was accordiugly sent to Paris in
1806. This was the beginning of the period when Austria,
humbled but not exhausted by the blow of Austerlitz and
by the losses accompanying the peace of Pressburg, deter-
mined, under the leadership of Count Stadion, to prepare
for another war on a greater scale. But the sudden over-
throw of Prussia, and the alliance between France and
Russia which was made at Tilsit in 1807, added immeasur-|
ably to the diffic\dties of the court of Vienna. It becamflt
clear that Napoleon was intending to dismember Tiurkey.i
and to gain for himself some part of the spoils of the Otto-
man empire. Metternich's advice was that Austria should
endeavour to detach the czar from the French alliance, and
by this means frustrate the plan of partition ; but, should
Russia hold fast to Napoleon, that Austria itself should unite
with the two aggressors, and secure its share of Turkey.
Oriental affairs, however, fell into the backgroimd, and|
in the summer of 1808 Mettemich was convinced that:
Napoleon was intending to attack Austria, though not im-j
mediately. He warmly supported Count Stadion's policy
in raising the forces of Austria to the hi^est strength;
and, althon^ he did not share the minister's hopes in a
200
MET'i^ERNICH
general rising throughout Germany, he expressed in his
despatches no distrust of the power of Austria to cop<'
with Napoleon. Tliis is the more singular because,
after the disastrous issne of the campaign of 1809,
Metternich seems to have taken credit for having
opposed the policy of war. Napoleon again captured
■Vienna ; the battle of Wagram was lost ; and after a long
negotiation Austria had to purchase peace by the cession
of part of Austrian Poland and of its tllyrian provinces.
Metternich, who had virtually taken Count Stadion's place
immediately after the battle of Wagram, was now installed
as minister of foreign affairs. The first striking event
that took place under his administration was the marriage
of Marie Louise, daughter of the emperor Francis, to his
conqueror Napoleon. To do justice to Metternich's policy
it must be remembered that the alliance of Tilsit between
France and Russia was still in existence, and that Austria
was quite as much threatened by the czar's designs upon
Turkey as by Napoleorfs o^vn aggressions. Metternich
himself seems, in spite of his denials, to have been the real
author of the family union between the houses of Hapsburg
and Bonaparte, — a most politic, if not a high-spirited
measure, which guaranteed Austria against danger from
the east, at the same time that it gave it at least some
prospect of security from attack by Napoleon, and enabled
Metternich to mature his plans for the contingency of an
ultimate breach between France and Russia. In 1812 this
event occurred. Metternich, in nominal alliance with Napo-
leon, sent a small army into southern Russia, allowing it to
be understood by the czar that the attack was not serious.
Then followed the annihilation of the French invaders.
While Prussia, led by its patriots, declared war against
Napoleon, Metternich, with rare and provoking coolness,
held his hand, merely atating that Austria would no longer
regard itself as a subordinate ally, but would act with all its
force on one side or the other. The result of tliis reserve
was that Metternich could impose what terms he pleased on
Russia and Prussia as the price of his support. The armies
of these two powers, advancing into central Germany,
proved no match for the forces with which Napoleon took
the field in the spring of 1 8 1 3 ; and the hard-fought battles
of Liitzen and Bautzen resulted in the retreat of the allies.
After the combatants had made an armistice, Met-
ternich teudered Austria's armed mediation, reqiuring
Prussia to content itself vnth the restoration of its territory
bast of the Elbe, and leaving Napoleon's ascendency in
fclermany almost untouched. Napoleon, after a celebrated
interview with Metternich, madly rejected terms so favour-
able that every Prussian writer has denounced Metternich's
proposal of them as an act of bitter enmity to Prussia.
On the night of the 1 0th of August the congress of Prague, at
which Austria, as armed mediator, laid down conditions of
peace, was dissolved. Metternich himself gave orders for
the lighting of the watch-fires which signalled to the
armies in Silesia that Austria had declared war against
Napoleon. The battle of Leipsic and the campaign of
1814 in France followed, Metternich steadily pursuing the
policy of offering the most favourable terms possible to
Napoleon, and retarding the advance of the allied armies
upon the French capital. Metternich had nMhing of that
personal hatred towards the great conqueror which was
dominant both in Prussia and in England ; on the contrary,
though he saw with perfect clearness that, until Napoleon's
resources were much diminished, no one could be safe in
Eiu-ope, he held it possible to keep him in check without
destroying him, and looked for the security of Austria in
the establishment of a balance of power in which neither
Russia nor Franco should preponderate, while Prussia
should be strictly confined within its own limits in northern
Germany. The assistance of the Austrian army, which j
was no doubt necessary to the allies, had, so far as related
to PriLssia, been dearly purchased. When, at the beginning
of 1813, Prussia struck for the freedom of Germany, its
leading statesmen and patriots had hoped that the result
of the war of liberation would be the establishment of
German unity, and thit the minor German princes, who
had been Napoleon's vassals since 1806, would be forced to
surrender part of their rights as sovereigns, and submit to
a central authority. This dream, however, vanished as
soon as Austria entered the field as an ally. It was no
part of Metternich's policy to allow anything so revolu-
tionary as Germen Unity to be established, least of all
under the influence of Prussian innovators. He made
treaties with the king of Bavaria and Napoleon's other
German vassals, guaranteeing them, in return for their
support against France, seimrate independence and sove-
reignty when Germany should be reconstructed. Accord-
ingly, though the war resulted, through Napoleon's
obstinate refusal of the terms successively offered to him,
in the limitation of France to its eai'lier boundaries and in a
large extension of Prussia's territory, the settlement »[
Germany outside Prussia proceeded upon the LLnts laid
down by Sletternich, and the hopes of unity raised in
1813 were disappointed. A German confederation was
formed, in which the minor sovereigTis retained supreme
power within their own states, while the central authority,
the federal diet, represented, not the German nation, but
the host of governments under which the nation was
divided. Metternich even ad\'ised the emperor Francis of
Austria to decline the old title of German emperor, dis-
liking any open embodiment of the idea of German unity,
and preferring to maintain the ascendency of Austria by
a gentle pressure at the minor courts rather than by the
avowed exercise of imperial rights. In this unprogressive
German policy Metternich was completely successful.
His great opponent. Stein, the champion of German unity
and of constitutional systems, abandoned his work in
despair, and refused the useless post of president of the
diet, which Metternich, with a kind of gentle irony, offered
to him.
The second branch of Mettemicli's policy in 181 3-1 i
was that which related to Italy. Following the old maxims
of Austrian statesmanship, Metternich aimed not only at
securing a large territory beyond the Alps trnt at making
the influence of Austria predominant throughout the Italian
peninsula. The promises of national indejiendence which
had been made to the Italians when they were called 'upon
to rise against Napoleon were disregarded. In the secret
clauses of the first treaty of Paris the annc.<ation of both
Lombardy and Venetia was guaranteed to Austria, and the
rest of Italy was divided into small states as of old.
Napoleon's return from Elba led to the downfall ofMurat,
who had been allowed to retain the kingdom of Nai>lcs, and
to the reunion of this coimtry with Sicily, under the Bourbon
Ferdinand. After the second overthrow of Napoleon,
Metternich endeavom-ed to make every Italian sovereign
enter into a league under Austria's jiresidency. Ferdinand
of Naples accepted the jiosition of vassal, but the pope and
the king of Sardinia successfully maintained their inde-
pendence. With the construction of the German federation,
and the partial construction of an Italian federation, both
under Austria's guidance, the first pait of Metternich's
career closes. Ho had guarded Austria's interests with
great skill during the crisis of 1813 and 1811. It was not
his own fault, but the faiJt of ages, that Austria's interests
were in antagonism to those of German and of Italian
nationality. Ho thought as an Austrian, and as nothing
else ; his task was to servo the house of Hapsburg, and this
ho did with signal ability and success. To denounce
Metternich as a kind of criminal, according to the practice
M E T T E R N 1 C H
201
of Pnissian writers, because he did not work for German
unity, is to ignore the existence of such a thing as state-
poUcy. Judged by the ordinary standards of practical
statesmanship, not by the philosophy of history,
Metternich's action in 1813 and 1814 was that of a very
superior man ; and the qualities of calmness and dexterity
whicli he displayed would have given an infinitely greater
effectiveness to the life of his great rival Stein, who in
patriotic and moral enthusiasm was so far above him.
The second part of Metternich's career, which extends
from 1815 to 1848, is that of a leader of European conser-
vatism. It is difficxUt to describe his attitude towards
almost all the great questions which were now arising
as any but one of absolute blindness and infatuation.
He acknowledged that exceptional circumstances in the
past had made it possible for England to exist under a
constitution ; he knew that France would not surrender
the Charia given to it by King Louis XVIII.; but in all
other great states he maintained that there were no alter-
natives but absolute monarchical government and moral
anarchy. His denunciations of liberals and reformers
everywhere and at all times are perfectly childish ; and in
many instances his hatred of change led him into errors
of judgment not surpassed in the annals of political
folly. When Napoleon fell, there was a prospect of the
introduction of constitutional government tliroughout a
great part of Eui'ope. King Frederick William, stimulat-
ing the efforts of tlie Prussian people against France by the
hopes of liberty, had definitely promised them a constitu-
tion and a general assembly. The czar had determined to
introduce parliamentary life into the kingdom of Px>!and,
and even hoped to extend it, after some interval, to Kussia.
The Federal Act drawn up for Germany at tlie congress of
Vienna declared that in every state within the German
league a constitution should be established. Against this
liberal movement of the age Metternich resolutely set his
face. Though wide general causes were at work, the
personal influence of the Austrian statesman had no small
share in prolonging the existence of autocratic government,
and in developing that antagonism between the peoples
and their rulers which culminated in the revolutions of
1848. The nature of the Austrian state, composed of so
many heterogeneous provinces and nationalities, no doubt
made it natural for its representative to defend and exalt
the i)rinciple of personal sovereignty, on which alone the
■unity of Austria was based ; the relation of Austria to Italy
rendered the growth of the sentiment of nationality a real
source of danger to the house of Hapsburg ; but Metternich's
abhorrence of constitutional and popular ideas was more
than the outcome of a calculating policy. He was not a
man of much faith, but one belief he held with all the force
of religious conviction, — namely, the belief that his own
task and mission in the world was to uphold established
authority. All efforts to alter the form or to broaden the
basis of government he cla.ssed under the same head, as
■works of the spirit of revolution ; and in one of his most
earnest writings he places side by side, as instances of evil
sought for its o\vn sake, the action of the secret societies
in Germany, tho Carbonaria of Italy, and the attempts of
the English to carry the Reform Bill. Working on prin-
ciples like these, and without the shadow of a doubt in
his'own wisdom, Bletternich naturally proved a great power
at a time when the sovereigns who had inclined to constitu-
tional id?as began to feel the difficulties in the way of
putting them into practice. Metternich's advice, tendered
with every grace of manner and with the most winning
and persuasive art, was indeed not hard for rulers to accept,
for he simply recommended them to give up nothing that
they had got. It was at the congress of Aix-la-Chapelle
(JSlSjLthatJhe retrograde tendency, which was now suc-
ceeding to the hopes of 1815, first gained expression. An
agitation among the students at the German universities had
caused some scandal in the previous year, and secret societies
had just been discovered in Russia. Metternich plied the
king of Prussia with arguments for withholding the national
representation which he had promised to his people, and
stimulated the misgivings which were arising in tho mind
of the czar, hitherto the champion of European liberalism.
A few months later the murder of Alexander's German
agent, Kotzebue, by a fanatical student gave Metternich an
excellent pretext for organizing a crusade against German
liberty. A conference of ministers was hold at Carlsbad.
The king of Prussia allowed his representative to follow
Metternich's lead. The resistance of Ihe constitutional
minor states proved of no avail ; and a series of resolutions
was passed which made an end of the freedom of tlic press
throughout Germany, and subjected the teaching and tho
discipline of the universities to officers of state. A commis-
sion was established at Mainz to investigate tho conspiracies
which Metternich alleged to have been formed for the over;
throw of all existing governments, and for thccrcation of a
German republic, one and indivisible In the following year
new articles were added by Metternich's direction to the
original Federal Act, the most important being one that
forbade the creation in any German state of an assembly,
representing the community at large, and enforced the
system of representation by separate estates or orders, each
possessed of certain limited definite rights, and all alike
subordinate to the supremacy of the crown. Metternich
would gladly have made an end of the parliamentary con-
stitutious which had already come into being in Bavaria and
tlie southern states ; but he was unable to attack flicm
openly, and had to confine himself to the advocacy ^of
strict monarchical principles through his representatives at
these courts. With regard to Prussia, however, lie ^vas
completely successful. Tho king of Prussia broke Iii->
promise of establishing a national re]>resentation, and
satisfied his conscience by creating certain powerless pro-
vincial diets, exactly as Metternich had recommended Kim.
Throughout Germany at large a .system of re|ircssioii was
carried out against the advocates of constitutional right
The press was silenced ; societies were dissolved ; prosecu-
tions became more and more common. AVhile Jlellcrnich
imagined himself to be stifling the spirit of discontent, he
was in fact driving it into more secret and more violent
courses, and convincing eager men that tho regencralion
of Germany must be sought not in the reform but in tllb!
overthrow of governments.
Meanwhile revolution broke out in Spain and llnly:
Ferdinand of Spain, who had restored despotism, w;is (•(im-
pelled, in March 1820, to accept the constitution of \V-\'l
which he had subverted. Tlie same constitution was
accepted a few months later by Ferdinand of N'aplc.<
Spain was outside Metternich's range, but his hand fell
heavily upon Naples. A congress of the great powcn was
held at Troppau in October 1820. Metternich, who wa.s
president, as he had been at Vienna, and continued to be in
later congresses, comiiietely won over the czar to his own
views. Resolutions in favour of an intervention, if neci-s-
sary by force of arms, against the Neapolitan liberal (.'ovcrn-
nienf were adopted by Austria, Russia, and Prussia, llioiigli
England and France held aloof. The congress wns then
adjourned to Laibach in Carniola, whither Ferdinand ofj
Naples was summoned, in order that ho might ninliato
between the powers and his people, and induce the latter
to give up a constitution which offended the three n' rtliern
courts. Ferdinand's journey and mediation were an iuipo^
ture as regarded the Neapolitans; he pretended that Iio
went to negotiate on behalf of his jjcople, when in fact his
intention was exactly the same as Metternich's, namely, tu
J<Vt _ 06
202
M E T — M E T
have absolute monarchy restored. The proceedings of
the congress at Laibach were a farce. A letter was
concocted by Metternich for King Ferdinand to send to
his subjects, informing them that the powers would not
permit the constitution to exist, and that, in default of
their submission, the allied courts would employ force.
The British Government, while protesting against the joint
action of the three powers as an assumption of international
-sovereignty, was perfectly willing that Austria', as a state
endangered by the Neapolitan revolution, should act on
its own account. Metternich, however, continued to treat
the Neapolitan question as the affair of Europe, and
maintained his concert with Russia and Prussia. Early
in 1821 an Austrian force, acting in the name of the allies,
entered central Italy. The armies opposed to it col-
lapsed, and the Austrians entered Naples on March 24.
But in the meantime a revolution broke out in Pied-
mont, which threatened to cut off the Austrians from
their sujiports, and to raise all Italy against them. For a
moment the bold action of Jletternich seemed to have
resulted in immense danger both to his own conservative
policy and t& the peace of Europe ; for it was believed that
the Piedmontese revolution would be' answered, not only
by a general Italian movement, but by a rising against
the Bourbons in France. The cloud, however, passed away.
Order was quickly restored in Piedmont ; Lombardy was
safely held by Austrian garrisons ; and the conclusion of
the Italian difficulties, in which Metternich had played a
very difficult part with great resolution and dexterity, was
his complete and brilliant personal triumph. No statesman
in Euro|ie at this moment held a position that could com-
pare with his own.
At the congress of Verona, held in 1822, the affairs of
Spain were considered by the powers. In the end, the
Spanish constitution was overthrown by a French invading
army ; but, though the arm employed was that of France,
the principle of absolutism which animated the crusade
was that which Metternich had made hLs own. A severe
theck, however, now met him in another quarter. Greece
had risen against Turkish rule in 1821. The movement
was essentially a national and a religious one, but Metternich
treated it as a Jacobinical revolt against lawful authority,
— confusing, or affecting to confuse, the struggle for national
independence with the shallow and abortive efforts of politi-
cal liberalism in Italy and Spain. Metternich's attitude
towards the Greeks was for some time one of unqualified
hostility. If, under the pressure of the Tilsit alliance, he
had once been willing that Austria should join Russia in
dismembering Turkey, he had now reverted to the principle
of maintaining Turkey at all costs against a Russian
advance southwards; and he attributed the Greek move-
ment to the efforts of Russian agitators unauthorized by
tlie czar, Tlis desire was that the sultan should deprive
Russia of all i)0ssible cause for complaint as regarded its
own separate interests, and so gain freedom to deal sum-
marily witli the Greeks. Metternich's hopes failed, partly
through the obstinacy of the Turks, partly through the
waverijig conduct of Alexander, and partly through the
death of C'astlereagh and the accession of Canning to
power. It was in great part owing to Canning's moral
support that Greece ultimately becarne an independent
state ; and the e.vtraordinary violence of Metternich's
language whenever he mentions this English statesman
marks only too well the opposite character of his aims.
No politician has left a more damning record against
him.self than Metternich in his bigoted abuse of Canning.
'Die Clock question, however, was only the first on which
the judgment of events was now beginning to declare itself
against Metternich and all his princiijlcs. The French
revolution of 1830 shattered the moral fabric which hu
had so proudly inaugurated, and in great part himself
raised, in 1815. The accord that grew up between
England and France now made any revival of the
kind of presidency that he had once held in Europe
impossible. He was indeed bold and rapid in throw-
ing troops into the papal territory when revolutionary
movements broke out there in 1831 and 1832, though war
with France seemed likely to result from this step. He
was as un.sparing as he had been in 1819 in suppressing the
agitation which after 1830 spread from France to Germany;
and the union of the three eastern courts wa.s once more
exhibited in the meeting of the monarchs which took place
at Miinchcngr'itz in 1833, and in a declaration delivered at
Paris, insisting on their right of intervention against
revolution in other countries. It was, however, the new
czar of Russia, Nicholas, who was now the real head of
European conservatism ; and the stubborn character, the
narrow, unimaginative mind, of this prince made it
impossible for Metternich to shape his purposes by that
delicate touch which had been so effective with his pre-
decessor. But in Austria itself Metternich continued
without a. rival. In 1835 the emperor Francis, with
whom he had worked for nearly thirty years, died.
Metternich, himself falling into the mental habits of old
age, remained at the head of the state till 1848. The
revolution of that year ended his political career. He
resigned office with the dignity of demeanour which had
n?ver failed him ; his life was scarcely safe in Vienna, and
the old man came for a while to England, which he had
not visi' d since 1794. Living on till June 1859, he saw
every f^-'eat figure of his earlier life, and many that had ap-
peared on the horizon since his own prime, pass away; and
a few more months of life would have enabled him to see
the end of that political order which it had been his bfe-
work to uphold ; for the army of Napoleon lU. was crossing
the Sardinian frontier at the moment when be died, and
before a second sum.mer had gone Victor Emmanuel had
been proclaimed king of Italy.
Metternich was a diplomatist rather than a statesman.
His influence was that of an expert manager of individuals,
not of a man of great ideas. All his greatest work was
done before fifty ; and at an age when most statesmen are
in the maturity of their powers he had become tedious
and pedantic. His private character was very lovable.
He was an affectionate if not a faithful husband, a
delightful friend, and a most tender father. The ex-
cessive egotism which runs through his writings gives
perhaps an impression of weakness which did not really
belong to his nature. Drawn by a firmer pen, the scene
in which he describes himself labouring in the German
conferences of 1820, while his favourite daughter was dying
in an adjoining room, would have been one of the most
affecting things in political biography. The man who
could so have worked and felt together must have pcssessed
no ordinary strength of character, no common force of self-
control.
The collection of Metternich's writings published by his family
under the title of Dcnktoiirdigkciieii, along with French and.
English editions, contains letters and despatches of great value.
The autobiography isnot always trustworthy, and must be read with
caution. Gentz's correspondence is of first-rate importance for the
years 1813-30. Original papers are also contained in varioua
German works upon particular events or movements, as in
Oncken for tlie negotiations of 1813 ; Welcker, Acgidi, Nauwcrck
for German affairs in 1819 and following years ; Prokesch von
Osten for Eastern affairs. (C.A. F.)
METZ, the capital of German Lorraine, and one of the
strongest fortresses in Europe, is situated at the confluenco
of the Moselle and the SeiUo, 80 miles to the north-west
of Strasburg, and 190 miles to the cast of Paris. It is
the seat of a military governor, the judicial and administra-
tive authorities uf Lorraine, a Roman Catholic bishop,
M E T Z
203
Protestant and' Jewish consistories, and a chamber of com-
merce. The general appearance of the town is quaint and
irregular, but there are aJso many handsome modem streets.
The Moselle flows through it in several arms, crossed by
fourteen or fifteen bridges. In the south-west comer of
the town is the esplanade, an extensive open space com-
manding a fine view of the fertile " Pays Messin " around
Metz. The most interesting of the ten city gates is the
Porte d'Allemagne or Deutsches Thor, a castellated structure
arected in 1445, and still bearing traces of the siege of
Charles V. Metz contains seven Roman Catholic churches.
two Protestant churches, aud a synagogue. The cathedral,
vrith huge pointed ^\-indows, slender columns, aud numerous
Hying buttresses, was begun in the lUth cciitur)-, and
finished in 154G, and belongs to the decadence of the
Gothic style. The Giothic churches of St Vincent aud St
Eucharius, and the handsome garrison-church, completed
in 1881, also deserve mention. Among secular buildings
the most important are the large covered market, the
town-hall, the palace of justice, the theatre, the governor's
house, and the various buildings for military purposes.
The public library contains 35,000 volumes, including an
1. Palace of Jtutlce.
Metz aDd Nei^hboarhood.
9. Prefecture. d. CathedraL 4. Town-HaQ and GoTeraor*s Hoiue.
extensive collection of works relating to the history of
Lorraine. In the same building is the museum, which
contains a picture gallery, a numismatic cabinet, and a
collection of specimens of natural history. Metz also
possesses several learned societies and charitable institu-
tions, a gymnasium, three sominaries, and a military
academy. The cemetery of Chambifere contains the graves
of 8400 French soldiers who died here in 1870.
The commerce and industry of Metz have not yet
entirely recovered from the blow inflicted by the with-
drawal of French capital in 1871. The principal articles
nX manufacture are leather, coarse cloth and canvas, gun-
powder, arms, needles, billiard tables, hats, and artificial
flowers. There are several large iron-Vorks in the neigh-
bourhood. The trade of Metz is chiefly carried on in
leather, timber, wine, brandy, liqueurs, beer, preserved
fruits, and hardwares. A large annual fair is held here.
The civil population of Metz, which, in 1869 amounted
to 48,066, sank in 1872 to 33,134. Since then it has
steadily increased, and in 1881 was 43,275, about half
of whom were Germans. The garrison of Metz consists
of 10,000 men, or including the surrounding forta
nearly 16,000. The total of 58,813 includes 17,000 Pro-
teatanta and 1600 Jews.
204
M E U — M E U
Sislory.—lUU, the Gallic DivoJurOra, was the chief town of the
Mcdioniatrici, and ivas also called by the Romaus Medioniatrica, a
D.imc fiom which the present form has been derived by contraction.
Ciesar describes it as one of the oldest and mo-t important towns
in Gaul. The Romans, recogni2ing its strategical impwtance,
fortified it and sujiplied it with water by an imposing aqueduct,
the remains of which still exist. Under the Roman emperors Metz
was connected by military roads with Toul, Langrcs, Lyons, Stras-
bucg, VtrJun, Khcims, and Treves. Christianity was introduced
in the 3d century of our era. In the middle of the .'ith century
t.'ie town was plundered by the Huns uuder Attila ; subsequently
it came into the possession of the Franks ; and in 512 it was made
the cajjital of Austrasia. On the partition of the Carolingian
realms in 843 Jletz fell to the share of the western kingdom as
the capital of Lorraine. Its bishops, whose creation reaches back to
the 4lh century, now began to be very powerful. Metz acquired
the privileges of a free imperial town in the 12th century, and
attained great commercial prosperity. In 1552 it fell into the
hands of the French through treachery, and was heroically and
successfully defended against Charles V. by the young duke of
Guise. It now saiik to the level of a French provincial town, and
its population dwindled from 60,000 to 22,000 (169S). At the
l.eace oi Westphalia Metz, with Tool and Verdun, was formally
ceded to France, in whose possession it remained for upwards of
two centuries. In August 1870 the successes of the German troops
compelled Marshal Bazaine and the French army of the Rhine
to seek shelter behind the fortifications of Metz, which was forth-
with subjected by the Germans to a -rigorous blockade. After an
investment of ten weeks, during which not a single shot was fired at
tho town, Bazaine capitulated, surrendering to the victors an army
of nearly 180,000 men, several hundred cannon, and an immense
quantity of military stores of all kinds. By the peace of Frankfort
in 1871 Metz was again united to the German empire. Marshal
Fabert and Generals Custine and Kellermann were natives of Metz.
As a fortress Metz has always been of the highest importance,
and it now ranks with Strasburg as one of the two great bulwarks
of the west frontier of Germany. The original town-walls were
rc()laccd by ramparts in 1550, and the citadel was built in 1566. In
1674 the works were reconstructed by the celebrated military
engineer Vauban. Under Napoleon 111. the fortress was strength-
ened to meet the demands of modern warfare, and since 1871 the
Germans have spared neither time nor money ic^ completing and
supplementing his plans. The present fortifications of Metz con-
sist of two lines — an inner circle of bastions and ramparts enclosing
the city itself, and an outer circle of large detached forts on the
surrounding hills. The inner line is strengthened by two citadels,
one of which is advanced as a tete-de-pont on the leit bank of the
Moselle. The outer circle consists of nine or ten large forts, con-
nected with each other by smaller fortifications and commanding
all the approaches to the city. They form a large fortified camp
with a circumference of 15 miles, within which are twelve villages
and numerous country-houses and farms. The most distant of
the outlying' forts is about 3^ miles from the cathedral. Their
nani'^s and positions may be seen on the annexed plan. Previous
to 1870 the fortress of Metz had never succumbed to an enemy,
k Sourcs 0/ /n/orma(ion.— Westphal, Qeschichte der SCudt ifett, 1875-78 ; Gcorg
Lang, ifrt! tind seine Uiitgebungen, 1883, and Stati&litch-topographisches Band-
iuch fur Lolhrinften. The official Gentian accountof the blockade.of MetzHn 1870
will be (ouiiil in tho history of tlie Franco-German war issued b.v tlie general
staff at Ueiiin. 1872 sq. A succinct account is given by Georg Lang, Die Kriegs-
opcralionen urn Ifeti im Jahr 1870, 2d ed., Metz, 1880.
MEULEN, Antony Francis van dek (1634-1690),
was called to Paris about 1666 by Colbert, at the instance
of Le Brun, to fill the post of battle painter to Louis XIV.
Born in 1634 at Brussels, he had at an early age eclipsed
his master Peter Snayers, and the works executed 'by him
for the king of France during the campaigns of Flanders
(1667) so delighted Louis that from that date Van der
Meulen was ordered to accompany him in all his expedi-
tions. In 1673 he was received into the French Academy,
and attained the grade of councillor in 1681. Lodged in
the Gobelins, richly pensiomed, and loaded with honours,
he died at Paris in 1690. Detached works from his hand
are to be seen in various collcctious, but he is best repre-
sented by the series of twenty-three paintings, mostly
executed for Louis XIV., now in the Louvre. They ihow
that he always retained his Flemish predilections in
point of colour, although in other respects his stylo was
modified by that of the French school.
Sea Mim. ii\idit. Acad, de Peinture. 1854 ; Descamps, Via des
Peintres Flamands.
MEURTHE-ET-MOSELLE, a department in the north-
east of France formed in 1871 out of those parts of the
old ile|iartments of Meurthe and Moselle which continued
French, and deriving its name from the two principal rivers
which water it. Prior to 1790 it belonged to ancient
Lorraine, or to one or other of the bishoprics of Toul, Metz,
and- Verdun. It lies between 5° 25' and 7° 5' E. long,
and 48° 25' and 49° 5' N. lat., and is bounded on the E.
by Alsace-Lorraine, on the N. by Belgium and the grand-
duchy of Luxemburg, on the W. by the department of
Meuse, and on the S. by that of Vosges. The superficial
a>3a is 2020 square miles. Geologically Meurthe-et-
Moselle has five well-marked regions following each other in
regular succession from east to north-west. On the frontier
of Alsace are the Vosges mountains, of Trias sandstone
((/res Vosgiemi), with a maximum elevation of 3000 feek
A narrow band of variegated sandstone tlivides the Vosges
from the second region, formed of ;-helly limestone, which
extends as far as the Mem-the on the north and the Moselle
on the west. The third region is formed by the variegated
marls which cover the rich saline strata of the neighbour-
hood of Nancy. The Jura limestones of the Lias and
OoUte, to the north-west and west of the department, form
the last two regions. Here there is a maximum elevation
of 1 400 feet, and the plateau of Briey stretches out towards
that of the Ardennes. Between the Vo.=pes and the
Ardennes the vaUey of the Moselle run.s from south to
north, forming the main artery of the department; tha
lowest level (370 feet) occurs where the river leaves it.
Only a small part of the drainage of Meurthe-^t-Moselle
flows into the Meuse. The Moselle runs north-west from
its entrance into the department as far as Toul ; north-east
from Toul to FrouarJ, where it receives its principal
affluent, the Meurthe, and becomes navigable ; north from
Frouard to Pagny-sur-MoseUe, passing to Pont k Mousson.
The principal affluents of the Moselle are the Madon and
the Orne on the left, and on the right, besides the Meurthe,
the Seille, which in one part of its course forms the
boundary of Alsace-Lorraine. The Meurthe, which flows
to the north-west from Eaou I'litape to Frouard, passes on
to Baccarat, Lun^ville, St Nicholas, and Nancy, and is
swelled on the right by the Vezouse and the Sanon, and
on the left by the Mortagne. The principal tributary of
the Meuse within the department is the Chiers, which takes
its course by Longwy and Longuyon. Chmatologically
Meurthe-et-Moselle belongs to the Vosgian region. Its
mean annual temperatm'e is 52' Fahr., being 2° Fahr.
lower than that of Paris (which has the same latitude).
The' thermometer in severe winters falls to 13° Fahr.,
while in summer it reaches 100° Fahr. This is to be
accounted for by the general elevation of the department,
the proximity of the mountains, the arrangement of the
vaUeys (which he open towards the north), and the dis-
tance from the sea.
More than half of tho department consists of culturable land, one-
fourth of forests, and one-tenth of meadow land. In 1878 tlicre
were 54,346 horses, more than 100,000 sheep, 85,000 pig.', 74,000
caltle, 15,000 goats, 21,000 dogs, and 17,000 hives of bees. The
crops for tho same year araotmted to 454,192 quarters of wheat,
37,500 quarters of barley, 35,078 quarters of rye, 670,884 qnartcra
of oats, 9,079,125 bushels of pot.itJCs, and 76.868 tons of beet-root.
Hops, tobacco, colza, hemp, and llax also occupy a considerable
area. The annual yield of the vineyards (56 SQuare miles in exteot)
exceeds £900,000 ; tho wines of Toul are the best The most
common fruit trees are the pear, tho apple, the walnut, the clierry,
and the plum. Of forest trees the oak and tho wj'ch-elm are most
frequent in the west of the department, the beech and the fir in
the Vosges. Tho French school of forestry has its seat at Nancy.
The metallurgic industry is highly developed, and has made vcrj-
rapid progress within the last few years. Even in 1872 there
was a consumption of 350,000 tons of coal, four-fifths of which
came from Saarbruck, and tho remaining fifth from Belgium. In
1877 the iron ore obtained amounted to 1,000,000 tons, of which
two-thirds came from tho beds near Nancy, tho remainder from
the neighbourhood of Longwy. In 1S80 Die department produced
a thirdof tho pig-iron made in France (more than 500.000 tonsl.
M E U — M E U
205
In 1877 the yield wm 43,000 tons. Besides blast-furnnces, forges,
and rolling-mills, there are manufactories of files and boring tools,
agricultural implements, and furniture. In the production of salt
the department holds the first rank in France ; the salt-bearing
tracts cover more than 160 square miles, the beds having a mean
thicknessof 65 feet. The principal salt-workiiig centres (St Nicolas,
Varacgeville, and RosiJres-aux-Salines) lie between Nancy and
Lun^ville ; the annual value of rock-salt and refined salt produced
exceeds £600,000; subsidiary to this production is an important
manufacture of soda salts. The other chemical products are
prnssiate of potash, bone-black, wax-candles, soap, and matches.
Stone quarrying and the manufacture of plaster and lime are also
important branches of industry. The flint-glass manufactory of
Baccarat, which employs nearly 1600 workmen, is well known ;
that of plate-glass at Cirey (with 1000 woi-kmen) produces plates
of great size. The faience manufactories of Luniville, Toul, aud
Loiigwy are important. Mention may also be made of the
manufacture of window-glass, watch-glasses, and drinkiug-glasses.
The tobacco manufacture at Nancy employs 1000 workmen ; tan-
ning, glove-making, hat-making in felt and straw, wool-spinning,
and the manufacture of army clothing are also carried on. Nancy
is i*enowued for its embroidery, which is, however, diminishing
in importance. It also pos.sesscs factories for cotton spinning
and cotton stuffs, and for Hosiery. The starch manufactories and
the breweries, especially that of Tantonville, the largest in France,
are highly productive. Nancy also carries on distilleries, grain-
mills, paper-mills, manufactories of pasteboard objects, and a large
printing establishment. The commerce of the depaitment is effec-
tively served by 300 miles of railway (the principal line being tha*'.
from Paris to Strasburg through Nancy), by a number of good roads,
and by sever.il navigable rivers and canals. The main waterway
is formed by the canal between the Marne and the Rhine, which
runs by Toul aud Nancy, and traverses the department from west
to east. This canal communicates with the Moselle, which is navig-
able from Frouard downwards, and with the new eastern camu,
which reascends the Moselle as far as Spinal, and which is intended
to unite the Meuso and the Moselle witli the Saflne and the Rhone.
The population of Meurthe-et-Mosclle in 1881 was 419,317 in-
habitants. It constitutes the diocese of Nancy, has its court of
appeal at Nancy, and forms a part of the district of the Bth army
corps (Chalons-sur-Marne). There are i arrondisseinenU (Nancy,
Brioy, Luneville, and Toul), 29 cantons, and 597 communes. The
capital is Nancy, and the other priucipal towns are Pont h Mousson,
formerly the seat of a university ; Longwy (6064), a fortified place ;
and Baccarat (6013), celebrated for its glass-works.
MEUSE, Maese, or Maas, a river of France, Belgium,
and Holland, discharging into the North Sea or German
Ocean, has a course (variously measured) of Bome 500 or
550 miles, about 300 miles lying within France. Kising in
the department of Haute-Marne (1342 feet), at a point
where the plateau of Langres borders on the Monts Faucilles,
it follows a winding course, first from south to north, then
to Dorth-west, and afterwards to north, across the depart-
ments of Vosges, Meuse, and Ardennes, passing by
Neufchateau, Vaucouleurs, Commercy, St Mihiel, Verdun,
Sedan, Jfezi^res, and Qivet. Katurally navigable below
Verdun, it has been made so from Troussey, where it meets
the canal which unites the Marne to the Rhine, and from
this point to Li^ge it admits vessels of from 6 to 7 feet
draught. After traversing a wide valley covered by green
meadows, the Meuse, below M6zi6res, flows through narrow
gorges confined between rocky walls 200 or 300 feet high,
formed by the plateau of the Ardennes. The hills of the
Argonne, by which it is hemmed in on its upper course,
prevent its receiving any important affluent before the
Chiers and the Semoy, which both fall into it on the right
in the Ardennes. At the point where it leaves France its
ordinary volume is about 1000 cubic feet, [n Belgium it
runs picturesquely between the districts of Famenne and
Condroz on the right, and those of Les Fagnes and Hesbaye
on the left. Above Dinant it receives the Lesse, whose
valley is celebrated for its wonderful grottoes, and at the
foot of the citadel of Namur it is joined on the left by its
principal affluent, the Sambre, whose north-easterly direction
it takes. It then takes its course through the busy valley
in which Huy, Seraing, and Li(5ge are situated, receiving
the Ourthe on its right. Resuming a northerly direction,
then taking one to the north-west, and finally one to the
west, the Meuse passes in front of the Dutch citadel of
Maestricht to Roermonde. so called from its continence
there with the Roer, and to'Venlo, where the canal between
the Meuse and the Scheldt begins. Flowing thence through
an absolutely unbroken plain, it finally joins the Rhine, to
which it gives its own name, although the volume of its
waters is twenty times less than that of the German river.
It is at Gorcum that the Waal, the first separate arm of
the Rhine, brings to the Meuse two-thirds of the waters
of that river. The Meuso soon after divides into two
branches. While the Merwede flows due west, the southern
arm falls into the Biesbosch, an estuary of the sea, formed
four hundred and fifty years ago by an irruption of the sea
over a coi'itry then cultivated and thickly peopled, and now
the subject of attempts at reclamation. On reaching
Dordrecht, where the river navigation and sea navigation
meet, and where the rafts which come down from the
Black Forest are broken up, the Meuse again divides into
two arms. The Old Meuse flows due west, while the
northern arm joins the Lek, a second branch of the Rhine,
and continues its coiu'se to Rotterdam. This is the most
important branch of the estuary of the Sleuse, and efforts
are being made to regulate and deepen its channel by con-
structing one of those grand canals in which the Dutch
are so skilful. Schiedam and Vlardingen, both on the
right, are the last places of importance on the banks of
the river.
MEUSE, a department in the north-east of France,
formed out of a part of Lorraine and portions of the Three
Bishoprics, the Clermontais, and Champagne, derives its
name from the river by which it is traversed from south
to north. It lies between 4° 52' and 5° 50' E. long., and
between 48° 25' and 49° 38' N. lat, and is bounded on
the N. by Belgium and the department of Ardennes, on
the E. by that of Meurthe-et^Moselle, on the S. by
those of Vosges and Haute-Marne, and on the W. by
those of Marne and Ardennes. Of its superficial area (2405
square miles), about one-half belongs to the basin of the
Meuse, which is enclosed to the east and west by the
eastern and western Argonnes. On the north-east it is
watered by the Orne, a tributary of the Moselle, and the
Chiers, which runs by Montm^dy, and joins the Meuse a
little beyond the northern limit of the department. The
other half sends its waters to the Seine through the Aire, a
tributary of the Aisne, both of which take their rise here,
and by the Ornain, an affluent of the Saux, these two last
being tributary to the Marne. The Meuse receives no
important river in its course through this department. The
highest elevation (1388 feet) occurs to the south-west, on
the line of the ridge which separates the basin of the
Meuse from that of the Seine. 'The heights gradually sink
from south to north, but seldom fall below 1000 feet. The
hiUs of the western Argonne similarly sink rapidly down to
the valley of the Saux, where the lowest level of the
department (377 feet) is reached. The climate of Meuse
is transitional between the region of the Seine and that of
the Vosges ; its winters are less severe than those of the
latter, but it is not so temperate as the former. The mean
annual temperature is 52° Fahr. As at Paris, the maximum
cold is 9° Fahr.; the greatest heat rarely exceeds 96'
Fahr.
More than half the sunace of the department consists of cultur-
oble lands, one-fourth of forest, one-tenth of meadow land. The
proportion of horses is larger than in any other French depart-
ment, except La Manche. There are 63,800 horses, 90,000 cattle,
146,000 sheep, 125,000 pigs, and nearly 30,000 beehives. Cereals,
potatoes, and beet-root are the chief crops (in 1877 466,966 quarters
of wheat, 104,660 quurters of barley, 685,365 quarters of oata,
7,677, 374 bushels of potatoes, besides pulse, hemp, and colza). The
vineyards produced more than 6,600,000 gallons of wine of good
quality. 'The forests, which are principally of oak, ire rich in
game, as are the rivers in iiab. The mineral ^ealtb of the depart-
20fi
M E X — M E X
I'ment includes ir»n ore, good freestone, and fossil phosphates of lime.
iThere are blast-furnaces, iron, copper, and bell foundries, wire-
[works, and manufactories of files, Imrdware, and edge tools. Tho
,cotton-spinning factories employ 15, 000 spindles and 32,000 frames ;
the woollen manufacLuro employs 0000 spindles, and some hundreds
of persons are employed in the spinning and weaving of hemp, flax,
and jute. The glass-works (particularly the manufactory of painted
window-glass, transferred alter the war of 1870 from Metz to Bar-
Je-Duc), paper-mills, saw-mills, and flour-mills, as well as the
manufactures of lime, tiles, and lire-bricks, arc worthy of mention.
Hosiery and embroidery also give occupation to a great nnmbcr of
workshops, and tho department is celebrated for its confectionery.
Meuse contains more than 300 miles of railway, — tlio principal lines
(being that from Paria to Strasbmg through Bai'-le-Duc and Com-
mercy, that from Paris to Metz through Verdnn, and the branch
line to the Meuse. Tho chief watenvays avo the canal connecting
tho Marno with the Rhine, and tho canal of tho Meuse ; tlie two
together have a length of 146 miles. The population of the depart-
ment in 1881 was 28ii,861,— a small number in proportion to
its extent, and with a tendency to decrease. Eccrcsiaslically it
foi-ms tho diocese of Verdun ; it has its court of appeal at Nancy,
and constitutes part of tluj district of tho army corps of Chalons.
sur-Marne. There are 4 anoiidissements, — Bar-le-Duc, Conimcrcy,
MontmcSdy, and Verdun, — 28 cantons, and 086 communes. Bar-
le-Duc (population in 1881, 17,435) is the capital; Commercy
has 5260 inhabitants and Moutmedy 3000 ; St Mihiel (6916), on
the Ifeuso, has good churches and some remarkable rocks, and is
tho seat of the departmental assize court.
EXICO
L ANcrEJfT jrexico.
THE name Mexico is connected with tho name ©f the
group of Aiilerican tribes calling themselves Mexica
(sing. Mexicalt), or Azteca. The word i.? related to or
derived from the name of the Mexican national war-god
Me.xitl, better known as Huitzilopochtli. The Aztecs from
the 12 th century appear to liave migrated from place to
place over the mountain-walled plateau of Annlmac, tho
country " by the water," so called from its salt lagoon.s, and
which i.s now known as the valley of Mexico. About 1325
they founded on the lake of Tezcuco the permanent settle-
ment of Mexico Tenochtitlan, which is still represented by
the capital city Mexico. The name JMe.xico was given by
the Spanish conquerors to tho group of countries over
,which the Aztec power more or less prevailed at tho time
pi the European invasion. Clavigero (Storia Antica del
'Messico, vol. i.) gives a map of the so-called " Mexican
'empire," which may be roughly described as reaching from
the present Zacatecas to beyond Guatemala ; it is notice-
able that both these names are of Mexican origin, derived
respectively from words for " straw " and " wood." Eventu-
ally Mexico and New Mexico came to designate the still
vaster region of Spanish North America, which (till cut
down by changes which have limited the modern republic
of Mexico) reached as far as the Isthmus of Panama on
the south and took in California and Texas on the north.
Mexico in this ivide sense is of high interest to the
anthropologist, from the several native American civiliza-
'tions which appear \vithm its limits, and which con-
Iveniently if loosely group themselves round two centres,
the Mexican proper and the- Central American.
When early in the IGth century the Spaniards found
their way from tho West India Islands to this part of the
mainland of America, they came in view of nations cultured
high above the level they had hitherto met with in the New
World. Here were not rude and simple tribes like the
islanders of the Antilles, but nations with organized armies,
official administrators, courts of justice, high agriculture
and mechanical arts, and, what struck tho white men
'especially, stone buildings whose architecture and sculpture
were often of dimensions and elaborateness to astonish the
builders and sculptors of Europe. How a population of
millions could inhabit a world whose very existence had
been till then unknown to geographers and historians, and
how its nations could have reached so high a grade of
barbaric industry and grandeur, was a problem which
naturally excited the liveliest curiosity of scholars, arid gave
rise to a whole literature. Hernandez and Acosta shared
tho opinion of their tune that tho gi-eat fossil bones found
in Mexico werte remains of giants, and it was argued that,
as before the deluge there v/cre giants on tho earth, there-
fore Mexico was peopled from tho Old World in ante-
diluvian times. On tho other hand the multitude of
native American languages suggested that the migration
to America took place after tho building of the tower of
Babel, and Siguenza arrived at tho curiously definite result
that the Mexicans were descended from Naphtuhim, son of
Mizraim and gTandson of Noah, who left Egypt for Mexico
shortly after the confusion of tongues. Although such
speculations have fallen out of date, it is to hb remembered
in their favour that they were stepping-stones to more valid
argunlent ; especially they induced the collection of native
traditions ancl invaluable records of races, languages, and
customs, which othei-vi^c would have been lost for ever.
Even in the present ceutury Lord Kingsborough was led
to spend a fortune in 2n-inting a magnificent compilation of
Mexican picture-writings and documents in his Antiquitiea
of ilexico by his zeal to prove the theory advocated by
(jlarcia a century earlier, that the Mexicans were the lost
tribes of Israel.
Real information as to the nations of Mexico beforb
Spanish times is very imperfect, but not altogether want-
ing. It is derived partly from inspection of the natives
themselves, their languages and customs, which may be
now briefly considered, before going on to the recollections
handed down in the native picture-WTitings ancl oral tradi-
tions. The remarks made by the accurate and experienced
observer Alexander von Humboldt, who had seen more
American tribes than almost any traveller, are still entitled
to the greatest weight. He considered the native
Americans of both continents to be substantially similar
in race-characters. Such a generalization will become
sounder if, as is now generally done by anthropolo-
gists, tho Eskimo with their pjTamidal skulls, dull
complexion, and flat noses are removed into a division
by themselves. Apart from these polar nomads, the
American indigenes group roughly into a single race
or division of mankind, of course with loCal variations.
If our attention is turned to the natives of Mexico especi-
ally, the imity of type will be found particularly close.
The native population of tho plateau of Mexico, mainly
Aztecs, may still be seen by thousands without any'trace of
mixture of Eiu-opean blood ; and the following description
may give a fair idea of their appearance.' Their stature is
somewhat low, estimated about 5 feet 3 inches, but ihey
are of muscular and sturdy build. Measurements of their ■
skulls show them mesoceiihalic (index about V8), or inter-
mediate between the dolichocephalic and brachyccphalic
(narrow and wide skulled) types of mankind. The face is
oval, with low forehead, high cheek-boni^s, long eyes
sloping outward towards the temples, fleshy lips, nose wide
and in some cases flatfish but in others aquiline, coarsely
moulded features, with a somewhat stolid and gloomy
expression. Thickness of skin, masking the muscles. Las
been thought tho cause of a peculiar heaviness in tho out-
lines of body and face ; the complexion varies from yellow-
brown to chocolate (about 40 to -13 in the anthropological
' Keferences may bo found in Bancroft, Native Baca "f the Pacific^
SlaUa, vol i. pp. 24, 673, 618, W6.
MEXICO
207
^cale) ; eyes black ; straight coarse glossy black hair ;
beard and moustache scanty. Among variations from
this typo may be mentioned higher stature in some districts,
and lighter complexion in Tehuantcpec and elsewhere. If
now the native Americans be compared with the races of
the regions across the oceans to their east and west, it will
be seen that their unlikeness is extreme to the races east-
ward of them, whether white Europeans or black Africans.
On the other hand they are considerably like the Mongoloid
l)eopIes of North and East Asia (less so to the Polynesians) ;
so that the tendency anrong anthropologists is now generally
to admit a common origin, however remote, between the
tribes of Tartary and of America. This original connexion,
if it may be accepted, would seem to belong to a long-past
period, to judge from the failure of all at..empt3 to discover
an affinity between the languages of America and Asia.
At whatever date the Americans began to people America,
they must have had time to import or develop the numerous
families of languages actually found there, in none of which
has community of origin been satisfactorily proved with
any other language-group, at home or abroad. In Mexico
itself the languages of the Nahua nations, of which the
Aj-.tec is the best-known dialect, show no connexion of
origin with the language of the Otomi tribes, nor either of
these with the languages of the regions of the ruined cities
of Central America, the Quiche of Guatemala and the Jfaya
of Yucatan. Indeed, within the Mexican limits, there are
various other languages which, so far as philological
research can at present decide, are independent of one
another. The remarkable phenomenon of nations so
similar in bodily make but so distinct in language can
hardly be met except by supposing a long period to have
elapsed since the country Avas first inhabited by the
ancestors of peo[)les whose language has since passed into
€0 different forms. The original j)eopling of America may
■well date from the time when there was continuous land
between it and Asia.
It would not follow, however, that between these remote
ages and the time of the discovery of the New World by
Columbus no fresh immigrants can have reached America.
We may put out of the question the Scandinavian sea-
rovers who sailed to Greenland about the 10th century, and
appear afterwards to have coasted New Fngland (see
America, vol. i. p. 706), but do not seem to have found their
way far enough southward for their visit to have any effect
on Mexico. But at all times communication has been open
from East Asia and even the South Sea islands to the west
coast of America. The imijortance of this is evident when
we consider that Japanese junks now drift over by the
ocean current to California at the rate of about one a year,
often with some of the crew still alive (see C. W. Brooks in
Bancroft, vol. v. p. 51 ; Overland ilonthli/, San Francisco,
187'2, J). 3.13). Further north, the Aleutian islands offer
a line of easy sea passage, while in north-east Asia, near
Behring's Strait, live Chukchi tribes who carry on inter-
course with the American side ; the presence of Eskimo in
this partof Asia (see Nordenskiiild, Voy. ofVega,\o\. ii.pp. 13,
81) is so plainly due to locaUmigration that it is neglected
in comparing the languages of the two continents. Asiatics
such as Japanese or Kurile Islanders, if they found their
way in small numbers to America and merged into native
tribes, might hardly leave descendants distinguishable
from the rest of the population even in the first genera-
tion, nor introduce their own language. Such assertions as
that the Guatusos of Costa Rica are a tribe with fair skin
and flaxen hair, and that Jajianese worjls may be detected
among the Indians of British Columbia, are examples of
uvidence which may be worth further sifting ; but in an
account like the present no proofs can be admitted unless far
.better authenticated than tliese. WHiat gives a more solid
interest to the question of Asiatic influence in America, w
that, though neither the evidence of features nor of language
has substantiated it, there are details of >[cxican civilization
which are most easily accounted for on tlic sup|)osition that
they were borrowed from Asia. They do not seem ancient
enough to have to do wrth a remote Asiatic origin of the'
nations of America, but rather to be results of comparatively
modern intercourse between Asia and America, probably
since the Christian era. Humboldt ( Vues ilex CordiUertc,
pL.xxiii.) compared the Jlexican calendar with that in use
in eastern Asia. The Mongols, Tibetans, Chinese, and
other neighbouring nations have a cycle or scries of twelve
animals, viz., rat, bull, tiger, hare, dragon, serpent, horse,
goat, ape, cock, dog, pig, which may possibly be an imita-
tion of the ordinary Babylonian-Greek zodiac familiar tc
ourselves. The Mongolian peoples not only count their'
lunar months by these signs, but they reckon the successive
days by them, rat-day, bull-day, tiger-day, ic, and also,
by combining the twelve signs in rotation with the ele-
ments, they obtain a means of marking each year in the
sixty-year cycle, as the wood-rat year, the fire-tiger year, (tc.
This method is highly artificial, consisting, not in mere
numbering, but in combining series of different terms so
that the same combination does not recur till the end of
the period. Thus the reajipearance of its principle in th«
Mexican and Central-American calendar (see p. 212) is sug-
gestive of importation from Asia. Humboldt also discussed
the Mexican doctrine, represented in the native pictures, of
four ages of the world belonging to water, earth, air, and
fire, and ending respectively by deluge, earthquake, tempest,
and conflagration. The resemblance of this to some
versions of the Hindu doctrine of the four ages or yuga is
of so remarkable a closeness as hardly to be accounted for
except on the hyiJOthesis that the Mexican theology con-
tains ideas learnt from Asiatics. Among Asiatic jioints of
resemblance to which attention has since been called is
the Mexican belief in the nine stages of heaven aad hell,
an idea which nothing in nature would suggest directly to
a barbaric people, but which corresponds to the idea
of successive heavens and hells among Brahmans and
Buddhists, who aiijiarcntly learnt it (in common with our
own ancestors) from the Babylonian-Greek astronomical
theory of successive stages or concentric planetary sjiherca
belonging to the jilancts, he. The Spanish chronicles
also give accounts of a Mexican game called patolli, played
at the time of the conquest with coloured stones moved
on the squares of a cross-shaped figure, according to the
throws of beans marked on on^ side ; the descriptions of
this rather complicated game correspond closely with the
Hindu backgammon called pachisi (see Tylor in Jour.
Anthrop. Inst., vol. viii. p. 116).'
The native history of Jlcxico and Central America is
entitled to more respect than the mere recollections of
savage tribes, inasmucli as here memory was aided by
something like written record. The Mexican pictures so
far approached writing pro)ier as to set down legibly the
names of persons and places and the dates of events, while
the rude drawings which accompanied these at least
helped the professional historians to remember the tradi-
tions repeated orally from generation to generation. Thus
actual documents of native Aztec history, or copies of
' Tie appendix to Prescott's Conquest of Mexico contains iin
interc-ting snnnnaj'y of an.'xlofrics Iietwcen the civilization of .Mexico
and tliat of the Old World, but sonic of the arguments arc very inra.n-
dusive. One whicli has lieeu oftin cited turns on the likeness alhigMl
l>y Naxcra between the Chinese lancuage and that of the Otomi nation
of V:Kico (whose name survives in that of their town Otoinjian, now
Otuniba). The examination of an Otonii grammar (such as Eli'inmtt
■de la. Grammaire Othomi, Paris, 18C3) will, however, convince the
philological reader that the resenihlance is haixUy of an amount fo
found a theory of a Chinese connexion upon.
208
MEXICO
them, are still open to the study of scholars, while after
the conquest interpretations of these were drawn up in
writing by Spanish-educated Mexicans, and histories
founded on them with the aid of traditional memory were
written by Ixtlilxochitl and Tezozomoc ; the most important
of these picture-writings, interpretations, and histories may
be found in Kingsborough's Antiquities of Mexico. In
Central America the rows of complex hieroglyphs to be
seen sculptured on the ruined tunii)Ies probably served
a similar purpose up to the time of the Spanish invasion.
The documents purporting to bo histories, written down
by natives in later times, thus more or less represent real
records of the past, but the Uisk of separating the preponder-
ant mythical part from what is real history is of the utmost
difficulty. Among the most curious documents of early
Amerioa is the Popo!-Vuh or national book of the Quiche
kingdom of Guatemala, a compilation of traditions ■written
down by native scribes, found and translated by Father
Ximenez about 1700, and pubUshed by Scherzer (Vienna,
1857) and Brasseur de Bourbourg (Paris, 1861). This
book, ' composed in a pictiu'eSque barbaric style, begins
with the time when there was only the heaven with its
boundaries towards the four winds, but as yet there was
no body, nothing that clung to anything else, nothing that
balanced itself or rubbed together or made a sound ; there
was nought below but the calm sea alone in the silent
darkness. Alone were the Creator, the Former, the Ruler,
the Feathered Serpent, they who give being and whose name
is Gucumatz. Then foUows the creation, when the creators
said "Earth," and the earth was formed like a cloud or a fog,
and the mountains appeared like lobsters from the water,
cypress and pine covered the hills and valleys, and their
forests were peopled with beasts and birds, but these could
not speak the. name of their creators, but could only chatter
and croak. So man was made first of clay, but he was
etrengthless and senseless and melted in the water ; then
they made a race of wooden mannikins, but these were
useless creatiires without heart or mind, and they were
destroyed by a great flood, and pitch poured down on them
from heaven, those who were left of them being turned
into the apes stiU to bo seen in the woods. After this
comes the creation of the four men and their wives who
are the ancestors of the Quiches, and the tradition records
the migrations of the nation to Tulan, otherwise cfdied the
Seven Caves, and thence across the sea, whose waters were
divided for their passage. It is worth while to mention
these few early incidents of the national legend of
Guatemala, because their Biblical incidents show how
native tradition incorporated matter learnt from the white
men. Moreover, this Central- American document, mythical
as it is, has an historical importance from its bringing in
names belonging also to the traditions of Mexico proper.
Thus Gucumatz, " Feathered Seri>ent," corresponds in name
to the Mexican deity Quetzalcoatl ; Tulan and the Seven
Caves are familiar W5ras in the Aztec miyration-traditions,
and there is even mention of a chief of Toltccat, a name
plainly referring to the famed Toltecs, of whom further
account will be given in their place in Mexican history.
Thus the legends of the Popol- Yuh confirm what is learnt
from comparing the ciJture of Central America and Mexico
proper, that, though the nations of these districts were not
connected by language, the intercourse and mixture
between them had been sufficient to implant in them much
■common civilization, and to justify the anthropologist in
including both districts in one region. Historical value of
the ordinary kind may be found in the latter paj-t of the
Popol- Vuh, which gives names of chiefs down to the time
when they began to bear Spanish names, and the great city
of Quich6 became the deserted ruin of Santa Cruz. The
Maya district of Yucatan has also some vestiges of native
traditions in the manuscript tsanslated by D. Pio Perez
(in Stephens, Incidents of Travel in Yucatan) and in tlie
remarkable 16th century Relacion de las Cosas de Yucatan,
by Diego de Landa, published by Brasseur de Bourboui'g
(Paris, 1864). As in the Guatemala traditions, we hear
of ancient migration from the Mexican legendary region
of Tula ; and here the leaders are four famous chiefs or
ance.stors who bear the Aztec name of the Tutul-Xiu, which
interpreted means " Bird-Tree." Unfortunately for the
historical standing of these four ancestors, there are in tiie
Aztec picture-\vriting3 representations of four trees each
with a bird perched on it, and placed facing the four
quarters, which make it probable that the four Tutul-Xiu of
tradition, in spite of the circumstantial detail of their wars
and migrations, may be only mythic per.sonifications of tlie
four cardinal points (see Schultz-Sellack in Zeitsck.f. Ethn.,
1879, p. 209). Nevertheless, part of the later Maya records
may be genuine, — for instance, when they relate the war
about three centuries before the Spanish conquest, when the
king of Chichen-Itza destroyed the great city of Mayapan.
Though the names and dates of Central-American native
kings have too little interest to general readers for traditions
of them to be dwelt on here, they Jiring into view one im-
portant historical point, that the wondrous ruined cities of
this region are not to be thought monuments of a perished
race in a forgotten past, but that at least some of them
belong to history, having been inhabited up to the conquest,
apparently by the very nations who built them.
Turning now to the native chronicles of the Mexican
nations, these are found to be substantial dated records
going back to the 18th or 13th century, with some vague
but not worthless recollections of national events from times
some centuries earlier. These last-mentioned traditions,
in some measure borne out by Linguistic evidence of names
of places, tribes, and persons, point to the immigration of
detachments or branches of a widespread race speaking »■
common language, which is represented to us by the
Aztec, still a spoken language in Mexico. This language
was called nahtuttl, and one who spoke it as his native
tongue was called nahuatlacatl, so that modern anthro-
pologists are following native precedent when they use the
term Nahua for the whole series of peoples now under
consideration.^ Earliest of the Nahua nations, the Toltecs
are traditionally related to have left their northern home
of Huehuetlapallan in the 6th century ; and, though this
remote date cannot be treated as belonging to genuine
history, there is other evidence of the real existence of the
nation. Their name Toltecatl signifies an inhabitant of
ToUan, " land of reeds," a place which, as has been already
pointed out, appears elsewhere in the national traditions of
this region, and has a definite geographical site in the
present Tulan or Tula, north of the valley of Anahuac,
where a Toltec kingdom of some extent seems to have had
its centre. To this nation is a-scribed not only the oldest
but the highest culture of the Nahua nations ; to them
was due the introduction of maize and cotton into Mexico,
the skilful workmanship in gold and silver, the art of build-
ing on a scale of vastncss still witnessed to by the mound of
Cholula, said to be Toltec work ; the Mexican hierogljiihic
writing and calendar are also declared to have been of
Toltec origin. With the Toltecs is associated the mysterious
tradition of Quetzalcoatl, a name which presents itself in
Mexican rehgion as that of a great deity, god of the air,
and in legend as that of a saintly ruler and civilizer. His
brown and beardless worshippers describe him as of another
raee, a white man with noble features, long black hair and
full beard, dressed in flowing robes. He came from Tullan
' It should bo noticwl Hint this word is not ctj-mologiciUy con-
nected with the somewhat similar word Anahxtac, ofj'hich the muni
ing U given at pitge 208.
MEXICO
209
or from Yucatan (for the stones differ widely), and dwelt
twenty years among them, teaching men to follow his
austere and virtuous life, to hate all violence and war, to
sacrifice no men or beasts on the altars, but to give mild
offerings of bread and flowers and perfumes, and to do
penance by the votaries drawing blood with thorns from
their own bodies, legend tells stories of his teaching men
picture-writing and the calendar, and also the artistic work
of the silversmith, for which Cholula was long famed ; but
at last he departed, some say towards the unknown land of
Tlapallan, but others to Coatzacualco on the Atlantic coast
on the confines of Central America, where native tradition
still keeps up the divine names of Gncumatz among the
Quiches (see p. 208) and Cukulcan among the Mayas, these
names ha,ving the same meaning as Quetzalcoatl in Aztec,
viz., " Feathered Serpent." Kative tradition held that
when Quetzalcoatl reached the Atlantic he sent back his
companions to tell the Cholulans that in a futiu'e age his
bretiren, white men and bearded like himself, should land
there from the sea where the sun rises, and come to rule
the country. That there is a basis of reality in the Toltec
traditions is shown by the word toltecail having become
among the later Aztecs a substantive signifying an artist
or skUled craftsman. It \a further related by the Mexican
historians that the Toltec nation all but perished in the
11th century by years of drought, famine, and pestUence,
a few only of the survivors remaining in the land, while the
rest migrated into Yucatan and Guatemala, where, as has
been already pointed out, their name is commemorated in
local records. After the Toltecs came the Chichimecs,
whose name, derived from chichi, "dog," is applied to
many rude tribes ; the Chichimecs here in question are
said to have come from Amaquemecan under a king named
Xolotl, names which being Aztec imply that the nation
was Nahua ; at any rate they appear afterwards as fusing
with more cultured Nahua nations in the neighbourhood
of Tezcuco. Lastly is recorded the Mexican immigration
of the seven nations, Xochimiica, Chalca, Tepaneca,
Acolhua, Tlahuica, Tlascalteca, Azteca. This classification
of the Nahnatlac tribes has a meaning and value. It is
true that Aztlan, the land whence the Aztecs traced their
name and source, cannot be identified by geographers, while
the story of the separation of the seven nations at the place
called Chicomoztoc or Seven Caves looks like national legend
rather than real history. But the later stages of the long
Aztec migration seem historical, and the map of Mexico
still shows the names of several settlements recorded in the
curious migration-map published by Gemelii Careri {Giro
del Hondo, Venice, 1728)and commented on by Humboldt;
among these local names are Tzompanco, " place of skulls,"
now Zumpango in the north of iha Mexican valley, and
Chapultepec, "grasshopper hill," now a suburb of the city
of Mexico itself, where the Aztecs are recorded to have
celebrated in 1195 the festival of tying up the "bundle of
years " and beginning a new cycle. The Aztecs moving
from place to place in Anahuac found little welcome from
the Nahua peoples already settled there, whose own history
was indeed one of incessant jealousy and quarrel. One of
the first clear events of the Aztec arrival is their being
made tributary by the Tepanecs, in whose service or
alliance they began to manifest their warlike prowess in
the fight near Tepeyaeac, where now stands the famous
shrine of Our Lady of Giiadalupe. Thus they overcame in
arms the Acolhuas, their superiors in civilization, who had
made Tezcuco a centre of prosperity and improvement.
By the 13th century the Aztecs by their ferocity had
banded their neighbours together against them ; some
were driven to take refuge on the reedy lake shore at
^coculco while others were taken as captives into
Oiilhuacan The king of this district was Coscoxtli,
16—10
whose name has gained an nndeeerved reputation even in
Europe as "Coxcox, the Mexican Noah," from a scene in
the native picture-writing where his name appears together
with the figure of a man floating in a dug-out tree^ which
has been mistaken even by Humboldt for a represen-
tation of the Mexican deluge-myth. Coxcoxtli used
the help of the Aztecs "against the Xochimilco people,
but his own nation, horrified at their bloodthirsty sac-
rifice of prisoners, drove them out to live for years in
want and misery on the islands and swamps of the
great salt lagoon, where they are said to have taken to
making their chinampas or floating gardens of mud
heaped on rafts of reeds and brush, which in later times
were so remarkable a feature of Mexico. As one of the
Aztec chiefs at the time of the founding of their city was
called Tenoch, i.e., "Stone-cactus," it is likely that from
him was derived the name Tenochtitlan or " StoneKjactns
place." Written as this name is in pictures or rebus, it
probably suggested the invention of the well-known legend
of a prophecy that the war-god's temple should be bnilt
where a prickly pear was found growing on a rcik, and
perched on it an eagle holding a serpent ; this legend is
still commemorated on the coins of Mexico. Mexico-
Tenochtitlan, founded, about 1325,' for many years after-
wards probably remained a cluster of huts, and the higher
civilization of the cou;itry was still to be found among the
other nations, especially among the Acolhuas in Tezcuco.
The wars of this nation with the Tepanecs, which went on
into the 15th century, were merely destructive, but larger
effects arose from the expeditions under the Culhua king
Acamapichtli, where the Aztec warriors were prominent,
and which extended far outside the valley of Anahuac.
Especially a foray southward to Quauhnahuac, now Cuer-
navaca, on the watershed between the Atlantic and Pacific,
caused the bringing of goldsmiths and other craftsmen home
to Tenochtitlan, which now began to rise in arts, the Aztecs
laying aside their rude garments of aloe-fibre for more
costly clothing, and going out as traders for foreign
merchandise. In the. 14th century the last great national
struggle took place. The Acolhuas had at first the
advantage, but Ixtlilxochitl did not follow up the beaten
Aztecs but allowed them to make peace, whereupon, under
professions of submission, they fell upon and sacked the
city of Tezcuco. The next king of Tezcuco, Nezahualcoyotl,'
turned the course of war, when Azcapuzalco, the Tepanec
stronghold, was taken and the inhabitants sold as slaves by
the conquering Acolhuas aSd Aztecs ; the place thus de-
graded became afterwards the great slave-market of Mexico.
In this war we first meet with the Aztec name Moteuczoma,
afterwards so famous in its Spanish form Monteziuna.
About 1430 took place the triple alliance of the Acolhua,
Aztec, and Tepanec kings, whose capitals were Tezcuco,
Mexico, and Tlacopan, the latter standing much below the
other two. In fact the Aztecs now became so predominant
that the rest of native history may be fairly called the
Aztec period, notwithstanding the picturesque magnificence
and intellectual culture which made Tezcuco celebrated
under Nezahualcoyotl and his son NezahualpiUi. When
the first Moteuczoma was crowned king of the Aztecs, the
Mexican sway extended far beyond the valley plateau of
its origin, and the gods of conquered nations around had
their shrines set up in Tenochtitlan in manifest inferiority
to the temple of Huitzilopochtli, the war-god of the Aztec
conquerors. The rich region of Quauhnahuac became
tributary ; the Miztec country was invaded southward to
the Pacific, and the Xicalanca region to what is now Vera
Cruz. It was not merely for conquest and tribute that the
fierce Mexicans ravaged the neighbour-lands, but they had
a stronger motive than either in the desire to obtain
multitudes of prisoners whose hearts were to be torn out
210
MEXICO
by the sacrificing priests to propitiate a pantheon of gods
■who well i^ersonified their bloodthirsty worshippers. The
desire for war-captives as acceptable victims is related to
have brought about an almost incredible agreement among
nations of the Mexican alliance, that they should from
time to time fight battles among themselves in order to
provide prisoners for the altars. Thus there was something
of the character of a religious war in the expedition made
in 1469 under AxayacatI as far down the isthmus as
Tehuantepec, whence the Mexican army came back with
loads of rich plu'^er and thousands of captives, and the
later ravaging of the Totonac region as far as the Atlantic,
■when the inhabitants were taken for sacrifice and their
land recolonized by Aztecs. Ahuitzotl left the Aztec
empire (as it is often somewhat ambitiously called) at the
height of apparent power, but the cruel oppression of the
subject regions had made their life ahnost unbearable, and
the second Moteuczoma, coming to a rule already liable to
break Up from within, weakened it still more by upholding
the class of chiefs or nobles against the common people
■who as warrior.^ and traders had in great measure made
the prosperity of the allied nations. The Mexicans had
long tried to subjugate the stubborn little nation of Tlax-
callan (Tlascala), which had obstinately held out, though so
hemmed in that for years the people lived ■without salt, this
being no longer to be had from the sea-coast. Moteuczoma
made a last effort to crush them, but in vain, and when
the Spaniards came they were there as ready-made allies
planted on the high road to Mexico. From the date when
the festival of the new cycle was first celebrated in
Chapultepec six 52-year periods had passed when in 1.507
the new fire symbolizing the beginning of a new cycle
■was kindled for the last time on the breast of a human
■victim. Rumours of the coming of the Europeans may
have before this date spread from Cuba, but in 1517
Cordova touched in Yucatan, and in 1518 Grijalva was
on the east coast of Mexico, and the Aztecs first met the
■white men, in whom they .saw, partly ■with hope and partly
with fear, the fulfilment of the prophecy that Quetzalcoatl
should one day return. With the Spanish conquest under
Hernando Cortes (see Coktes) the native history of Mexico
coirfes to an end.
CrvnizATioN.
Goverr- While the prairie tribes of America lived nnder the loose
dent. sway of chiefs and councils of old men, the settled nations of
M«xico had attained to a somewhat highly organized government.
This may be seen by the elaborate balance of power maintained in
tlie federation of Mexico, Tezcuco, and Tlacopan, where each king
wae absolute in his own country, but in war or other pubhc interests
ihey acted jointly, with powers in something like the proportion in
which they divided conquered lands and spoil, which was two-fifths
each to Mexico and Teiicuco and one-fifth to Tlacopan. The suc-
cessor of the Aiitec king was customardy a chosen brother or nephew,
ttw eldest having the first claim unless set aside as incompetent,
a^d having to be a tried warrior ; this mode of succession, which has
bwn looked on as an elaborate practical device for secluding practical
aflTautages, seems rather to have arisen out of the law of choice
among the descendants of the female line, found in American tribes
of much lower culture. Something like this appears in the succcs-
aoa of kings ot Tezcuco and Tlacopan, which went to sons by the
pnncipal wife, who was usually of the Azioc royal family. The
jSSexican chronicles, however, show instances of the king's son suc-
ceeding, yr of powerful chiefs being elcctt'd to the kingship. The
tdm republic is sometimes used to describe the little state of
Tloscala, but this was in fact a federation of four cbiefs, with an
assembly of nobles. In the Zapotec district the Wiyatao or high-
priost of Zopaa was a divine ruler before whom all prostrated them-
sdv«s with faces to the ground ; he was even too sacred to allow
his foot to touch the earth, and W.1S only seen carried in a litter.
Palace:, The acoounts given by the Spanish and native Mexican writers' of
&c. the courts and palaces of the native kings must be taken with some
icsarre, froih the tendency to use descriptive terms not actually
iMttrue, but which convey erroneous ideas taken from European^
a'ltetccture ; thus what are called columns of porphyry and jasper
supporting marble balconies might perhips be better described as
piti's carrying slabs, while the apartraeiits and tornuM muit have I
been more remarkable for number and extent ;han architcctui»l
grandeur, being but low one-storied buildings. The principal
palace of Mexico consisted of hundreds of rooms and halls ranged
round three open squares, with women's apartment?, granaries/
storehouses, menageries, aviaries, of such extent that one of the
companions of Cortes records having four times wandered about
till he was tired, without seeing the whole. Not less remark-
able was the palace of Tezcuco, surrounded with its groves and
iileasure -gardens ; and, though now hardly anything remains of the
buildings above ground, the neighbouring hill of Tezcotrinco still
has its stone steps and terraces ; and the immense embankment
carrj'ing the aqueduct-channel of hewn stone which supplied water
to basins ciit in the solid rock still remains to prove that the chron-
iclers' descriptions, if highly-coloured, were at any rate geuuine. Till
the last centtuy the gigantic figure-s of AxayacatI and his son Monte-
zuma were to be seen carved in the porphj-rj' hill of Chapultepec,
but these as well as the hanging gardens have been destroyed, and
only the groves of ahuehucU (cypress) remain of the ancient beauties
of the place. That in the palace gardens flowers from the tierra
caliente were transplanted, and water-fowl bred near fresh and salt
pools fit for each kind, that all kinds of birds and beasts were kept
in well-appointed zoological gardens where there were homes even
for alligators and snakes, — all this testifies, not merely to barbaric
ostentation, but to a cultivation of natural histon,- which was really
beyond the European level of the time. From the palaces and re-
tinues of thousands of servants attached to the royal service may bo
inferred at once the despotic power ot the Mexican rulers and the
heavy taxation of the people ; in fact some of the most remarkable
of the picture-writings are tribute-rolls enumerating by hundreds
and thousands the mantles, ocelot-skins, bags of gold-dust, bronze
hatchets, loads of chocolate, &c. , furnished periodically by the towns.
Below the king was a numerous and powerful class of nobles, the
highest of whom (tlatoani) were great vassals owing little more than
homage and tribute to their feudal lord, while the natoral result
of the unruliness of the noble class was that the king to keep them
in check increased their numbers, brought them to the capital aa
councillors, aud balanced their influence by military and household
otEcers, and by a rich and powerful merchant class. The noUes
not only had privileges of rank and dignitj', but substantial power
over the plebeian or peasant class {macehualli), who submitted to
much the same oppression and ejctortion at their hands aa was
customary in the Old World. The tenures of land in Mexico were
those generally appearing in barbaric countries where invasion and
mihtary despotism have encroached on but not. totally superseded
the earlier tribal laws. The greatest estates belonged to the king,
or had been granted to military chiefs whose sons succeeded them,
or were the endowments of temples, hut the calpulH or village
commuiuty still survived, and each freeman of the tribe held and
tilled his portion of the common lands. Below the freemen were
the slaves, who were war-captives, persons enslaved for punishment,
or children sold by their parents. Prisoners of war were mostly
doomed to sacrifice, but other classes of slaves were mildly treated,
retaiiung civil rights, aud their children were born free.
The superior courts of law formed part of the palace, and there Justiot
were tribunals in the principal cities, over each of which presided &
supreme judge or cihiiacoatl, who was irremovable, and whose
criminal decisions not even the king might reverse ; he appointed
the lower judges and heard appeals from them ; it is doubtful
whether he judged in civU cases, hut both kinds of suits were heard
in the court below, by the ilacatccali and his two associates, below
whom were the ward-magistrates. Lands were set apart for the
maintenance of the judges, and indeed nothing gives a higher idea
of the elaborate civilization of Mexico than this judicial system,
which culminated in a general court and council of state presided
over by the king. The laws and recoids of suits were set down in
Sicture-writings, of which some are still to be seen ; sentence of
eath was recorded by drawing a line with an arrow across the
portrait of the condemned, and the chroniclers describe the barbaric
solemnity with which the king passed sentence sitting on a golden
and jewelled throne in the divine tribunal, with one hand on an
orn.aincnted skull and the golden arrow in the other. Among tho
resemblances to Old-World law was tho use of a judicial oath, tho
witness touching tho ground with his finger and putting it to his
lips, thus swearing by Mother Earth. The criminal laws were of
extreme severity, even petty theft being puirishcd by the thief being
enslaved to the person he had robbed, while to steal a tobacco
pouch or twenty ears of com was death ; he who pilfered in tho
market was then and thorcheaten to de.ith, and he who insulted Xipe,
the god of the gold- and silver-smiths, bv stealing his precious metal,
was skinned alive and sacrificed to tho olTendcd deity. Thouj;h
aloe-beer or "puhiue" was allowed for feasts aud to invalids in
moderation, and old people over seventy seem to be represented
in one of the picture-writings as having liberty of drunkenness,
youug men found drunk were clubbed to death and young womcu
stoned. Such a Draconian standard prevailing, ii is hardly needful
to enumerate the special penalties of such offcncd as witchcraft,
fraud, reuioviiig landmarka, adultery, Stc., which differed aa to
MEXICO
211
whether the criminal had hia heart cnt out on the altar, his head
crushed between two stones, &c. ; while even lesser punishments
were harsh, such as that of slanderers, whose hair was singed with
a nine-torch to the scalp. , . ^ , . , j -.i. »i.
Vii Based on conquest as the Ajitec kingdom was, and with the
cravin" for warlike glory fostered by the most bloodthirsty religion
the world ever saw, it follows that the nation was above all other
pursuits organized as a fighting community. To be a tried soldier
was the road to honour 4nd office, and the king could not be en-
throned till he had with his own hand taken captives to be
butchered on the war-god's altar at his coronation. The common
soldici-3 were promoted for acts of daring, and the children of chiefs
wove regularly trained to war, and initiated by being sent into
battle with veterans, with whoso aid the youth took his first prisoner,
but Ilia future rise depended on how many captives he took un-
aided in fight with warlike enemies ; by such feats he gained the
dignity of wearing coloured blankets, tassels, and lip-jewels, and
reached such military titles as that of "guiding eagle." The
Mexican military costumes are to be seen in the picture-writings,
where the military orders of princes, eagles, and tigers are known
by their braided hair, eagles' beaks, and spotted armour. Tlio
common soldiers went into battle brilliant in savage war-paint, but
those of higher rank had helmets like birds and beasts of prey,
armour of gold and silver, wooden greaves, and especially the
ichcapilli, the quilted cotton tunic two fingers thick, so serviceable
as a protection from arrows tliat the Spanish invaders were glad to
adopt it. The archers shot well and witli strong bows, though their
arrows were generally tipped only with stone or bone ; their shields
or targets, mostly round, were of ordinary barbaric forms ; the
spears or javelins had heads of obsidian or bronze, and were some-
times hurled with a spear-thrower or allatl, of which pictures and
specimens still exist, showing it to be similar in principle to those
nsed by the Australians and Eskimo. The most characteristic
weapon of the Mexicans was the maquahuill or " hand-wood," a
dub set with two rows of large sharp obsidian flakes, a well-
directed blow with which would cut down man or horse. These
two last-mentioned weapons have the look of highly-developed
savage forms, while on the other hand the military organization was
in some respects equal to that of an Asiatic nation, with its
regular companies commanded each by its captain and provided
with its standard. The armies were very large, an expedition often
consisting of several divisions each numbering eight thousand men,
but the tactics of the commanders were quite rudimentary, consist-
ing merely of attack by arrows and javelins at a distance, gradu-
ally closing into a hand-to-hand fight with clubs and spears, with
an occasional feigned retreat to draw the enemy into an ambuscade.
Fortification was well understood, as may still be seen in the
remains of walled and escarped strongholds on hills and in steep
ravines, while lagoon-cities like Mexico had the water approaches
defended by fleets of boats, and the causeways protected by towers
and ditches ; even after the town was entered, the pyramid-
temples with their surrounding walls were forts capable of stubborn
resistance. It was held unrighteous to invade another nation with-
out a solemn embassy to warn their chiefs of the miseries to which
they exposed themselves by refusing the submission demanded, and
this again was followed by a declaration of war, but in Mexico as
in other more cnlturcd countries this act of national morality degene-
rated into a ceremonial farce, where tribute was claimed from some
neighbouring nation, or an Aztec god was ofl"ered to be worshipped
in their temples, in order to pick a quarrel as a pretext for an
Invasion already planned to satisfy the soldiers with lands and
plunder, and to meet the priests' incessant demands for more human
sacrifices.
Beligion. Among the accounts of the Mexican religion are some passages
referring to the belieT in a supreme deity. The word teotl, god, has
been thought in some cases to bear this signification, but its me.ining
is that of deity in general, and it. fa applied not only to the sun-
god but to very inferior gods. It i- related that Nezahualcoyotl,
the poet-king of Tezcuco, built a nine-storied temple with a starry
roof above, in honour of the invisible deity called Tloquenahuaque,
"he who is all in himself," or Ipalnemoan, "he by whom we live,"
who had no image, and was propitiated, not, by bloody sacrifices, but
by incense and flowers. Those who adopt the opinion of Asiatic
admixture in Mexican culture will use it to account for this remark-
able religious phenomenon, less easily accounted for by native
development, while also the appearance of a rival deity of evil,
bearing the name of Tlacatecolotl, or "man-owl," is mysterious.
These divinities, however, seem to have had little or no place in the
popular faith, which was occupied by polytheistic gods of more
ordinary barbaric type. Tezcatlipoca was held to be the highest of
these, and at the festival of all the gods his footsteps were expected
to appear in the flour strewn to receive this sign of their coming.
He was plainly an ancient deity of the race, for attributes of many
kinds are crowded together in him, and he was ^ .ayed to in inter-
minable formulas for help in war and for health and fortune, to
deliver the nation from a wicked king, or to give pardon and strength
to the penitent who had confessed his sins and been purified by wash-
ing. Between him and Quetzalcoatl, the ancient deity of Cholti]a,
there had been old rivalry, as is related in legends of Quetzalcoatl
coming into the land to teach men to till the soil, to work metals, and
to rule a well-ordered state ; the two gods played their famous match
at the ball-game, and Tezcatlipoca, in the guise of a hoary-headed
sorcerer, persuaded the sick and weary Quetzalcoatl to drink the
magic pulque that sent him roaming to the distant ocean, where
he embarked in his boat and disappeared from among men. These
deities are not easily analysed, but on the other hand Tonatiuh and
Metztli, the sun and moon, stand out in the distinctest personalis
as nature gods, and the traveller still sees in the huge adobe |^aDii(&
of Teotih&acan, with their sides oriented to the four quarters, an
evidence of the importance of their worship. The war-god Huitzilo-
pochtli, of whom one legend relates a supernatural conception in
the ancient Tullan, while another storj' declares him to have been
(like the Chinese war-god) a deified warrior-chief, was the real head
of the Aztec pantheon ; his idol remains in Mexico, a huge block o£
basalt on which is sculptured on the one side his hideous personage,
adorned with the humming-bird feathers on the left hand which
signify his n.ame, while the not less frightful war-goddess Teoyao-
miqui, or "divine-war-death," occupies the other side. Centeotl,
the goddess of the all-nourishing maize, was patroness of the earth
and mother of the gods, while Mictlanteuctli, lord of dead-land,
ruled over the departed in the dim under-world. Kumbers of
lesser deities presided over classes of society, events, and occupations
of life, such as Tlazolteotl, goddess of pleasure, worshipped by
courtesans, Tezcatzoncatl, god of strong drink, whose garment in grim
irony clothed the drunkard's corpse, and Xipe, patron of the golJ-
smithi!. Below these were the usual crowd of nature-spirits of hills
and groves, whose shrines ^yere built by the roadside to receive oflTer-
ings from passers-by. The temples were called tcocalli or " god's
house," and the teocallis of the greater deities rivalled in size
as they resembled in form the temples of ancient Babylon. They
were pyramids on a square or oblong base, rising in successive
terraces to a small summit-platform. The great teocalli of
Huitzilopochtli in the city of Mexico stood in au immense
square, whence radiated the four principal thoroughfares,
its courtyard being enclosed by a square, of which the stone
wall, called the coatepantli or serpent-wall from its sculptured
serpents, measured nearly a quarter of a mile on each side. In
the centre, the oblong pyramid of rubble cased with hewn stone
and cemented, 375 x 300 feet at the base, and rising steeply in five
teiTaces to the height of 86 feet, showed conspicuously to the city
the long processions of priests and victims winding along the
terraces and up the corner flights of steps. On the paved platform
were three-story tower temples in whose ground-floor stood the stone
images and altars, and before that of the war-god the green stone of
sacrifice, humped so as to bend upward the body of the victim that
the priest might more easily slash open the breast with his obsidian
knife, tear out the heart and hold it up before the god, while the
captor and his friends were waiting below for the carcase to be
tumbled down the steps for them to carry home to be cooked for the
feast of victory. Before the shrines reeking with the stench of
slaughter, the eternal fires were kept burning, and on the platfonn
stood the huge drum covered with snakes' skin, whose fearfuj sound
was heard for miles. From the terrace could be seen seventy or
more other temples within the enclosure, with their images and
blazing fires, and the tzompantli or "skull-place," where the skulls
of victims by tens of thousands were skewered on cross-sticks or
built into towers. There also might be seen the flat circular
temalacatl or "spindle-stone," where captives armed with wooden
weapons were allowed the itockery of a gladiatorial fight ngainst
welfarmed champions. The great pyrataid of Cholula with
its hemispherical temple, of Quetzalcoatl at the top, now an
almost shapeless hill surmounted by a church, was about thrico
as long and twice as high as the teocalli of Mexico. A large
fraction of the Mexican population were set apart as priests or
attendants to the services of the gods. The rites performed were
such as are found elsewhere, prayer, sacrifice, processions, dances,
chants, fasting and other austerities, but there are some peculiari-
ties of detail. Prayers and other formulas have been copied down
by Sahagun and other chroniclers, of endless prolLxity, but not
without occasional touches of pathos. The following are a few
sentences from a prayer to Tezcatlipoca, interceding for the poor:
"O our lord, protector most strong and compassionate, invisible
and impalpable, thou art the giver of life ; lord of all, and lord
of battles, 1 present myself here before thee to sny some few words
concerning the need of the poor people, the people of none estate or
intelligence. . . . Know, O Lord, that thy subjects and servants
sufi'er a sore poverty, that cannot be told of more than thai
it is a sore poverty and desolatencss. The men have no garments
nor the women to cover themselves with, but only rags rent in
every part that let the wind and cold in. . . . If they be mer-
chants, they now sell only cakes of salt and broken pepper ; the
people that have something despise their wares, so that they go out to
sell from door to door and from house to house ; and when, they sell
nothing they sit down sadly by some fence, or waU, or in some comei^
212
MEXICO
licWftg their lips and gniwino.their naija for tlio binpf th»t u in
thom, they look on one side and the othefat the nouths of those who
jiass by, hoping perad venture that one may speak some word to them.
O com f tauiiynutu C'od, the bed on which tnoy lie is not a thing to rest
npon, but to endure torment in ; they draw a rag over tlioin at
night and so sleep. . jT.* O our Lord, in whose jjower it is to give
alicoM tent, con.Hofationf; sweetness, softness, prosperity, and riches, for
thou alone art lord of all good, have mercy upon them, for they are
thy scrvantt. ... I sHpi)licatc thee that tnou wilt lift up their
heads with thy favour ancl aid, that thou wilt see good that they
enjoy some days of prosperity and tranquillity, so^that they may
sleep and knonr repose, having prosperou-s and peaceable d.iys of
life. . . . .Should this nation, for whom I pray and entreat thee to
do them good, not understand what thou hast given, thou canst
t».ke away the good and pour out cursing, so that all evil may come
upon them, and they become poor, in need, maimed, lame, blind,
and deaf ; then indeed they shall waken and know the good that
they had and livive not, and they shall call upon thee and lean
toward thjce; but thou will not listen, for in the day of abundance
they would not understand thy goodness towards them." The^o
prayera aeern e.s.sentially genuine ; indeed there waa no Europiean
piodol from which they could have been imitated ; but at the sumo
time it mu.st be rememborod that they come down in Spanish writ-
ing, and not untouched by SpanLsh iu'tiuenco, as in one passage
where there It a mention of sheep, an animal of courseiiunknown to
the native Mexicans. As to sacrilico, maize and other vegetables were
oifered, and occasionally rabbits, quails, &.c. ; but, in the rbsence of
cattle, human eacriiiee was the chief rite, and cannibalism prevailed
at the feasts. Incense was constantly used, ospocially the copalli
(copal) well known to us for varnish ; little torra-cotta censers are
among the commonest of Mexican antiquities. l*ong and severe
religious fasts wore customary at special 'seasons, and drawing blood
from the arms, legs, and body, by thrusting in aloe-thorns, and
passing sharp sticks through the tongue, was an habitual act of
devotion recalling the similar ])r.'ietices of devotees in I-idia. The
calendar of religious festivals for the whole coiu^e of the Mexican
year has been preserved. Each 20-day period had one or more
such celebrations. In the month of the " diminishing of waters "
the rain-gods or Tlalocs were propitiated by a procession of priests
with music of flutes and trumpets carrying on plumed litters infants
with paitit^-d faces, in gay clothing with coloured paper wings, to
bo saerihcwl on tho mountains or in a whirlpool in tno lake. It is
fiaid that tlie people wept as they passed by ; but if so this may have
been a customarv formality, for tno religjon of these nations must'
have quenched all human sympathy. In tlie next month the god
Xipe-totec, already mentioned, had his festival called the "flaying of
men " from the human victims being flayed, after their hoarU were
torn out, for young men to dress in their skin^ and perform dances
and sham fights. The succeeding festival of Camaxtli was marked
by a severe fast of the priests, after whieh stone knives were pre-
pared with which a hole was cut through tho tongue of each, and
numbers of sticks passed through. For tlie great festival of Tez-
catlinoca, tlio handsomest and noblest of tho 'raptives of the year
.Tiad oecn chosen as the incarnate representative of the god, and
paradcnl the .streets for public adoration dressed in an embroidered
mantle witii iValhcrs and garlands on his head and a retinue like a
V\ng ; for the last month they married him to four girls representing
four goddesses ; on tho last day wives and pages escorted him to tho
little temple of Tlncochcalco, where ho mounted the stairs, breaking
an carthenwai-e flute against each step; this was a symbolic fare-
well to the joys of the world, for as he reached the top ho was
seized by the priests, his heart torn out and held up to tho sun,
liis head spitted on the tzompantli, and his boily eaten as sacred
food, the pc'oplo drawing from his fate tho moral lesson that riches
and pleasure may tirrn into poverty and sorrow. Tho manner of
the victim's death in these festivals afforded scope for variety; they
dressed thoni and made them daneo in character, throw them into
the liro for tlie fire-god, or crushed them between two balanced
stones at the harvest-festival. Tho ordinary pleasures of festivals
Were mingled "R-ith all this, such as dances in boast-masks, sham
fights, and children's games, but tho type of a religious function
was n sickening butclicry followed by a cannibal fea-st.
Picture- Tho Mexican priesthood, being the educated class, were much
wiitiug concerned with the art of picture-writing, which they had developed
to a stage quite above tho rude figures of tho American huntirtg-
tribes, and used systematically as a means of recording religious
festivals and legends, as well as keeping calendars of years and
recording the historical events which occurred in Ihcni. Fac Himilcs
of several of these interesting documents, witJi their tianslatious,
may be »m\ in Kingsborough. On inspecting these it will be .mcii
that their main ]iriuci])lo is ]>ictorial. Clods are represented with their
appropriate attributes, — tho fire-god hurling his spear, iho moon-
goddess with a shell, Jic. ; the scenes of human life are pictures of
warriors (ightiug with club and spear, men paddling in canoes, women |
spinning and weaving, &c. An in\portant step towards phonetic
writingappcai-s, however, in the picturonamcs of places and persons,
'i'lic siiriiilcat fonns of ;hese depict the objects sigiliBed by the name.
as where Chapulupte ot "grassboppcr-hill" is represented by BeratB.
hoppr ou a hilj, or a stone with a eactns on it stands for Teruek
or ' stone-cactus," tho founder of Tenochtillan. ■ Tho system had,
however, risen a etago beyond this when objects were drawn
to represent, not themselves, but the syllables forming their
names, as where a trap, an eagle, a pricker, and a hand are put to-
gether not to represent these objects, but in order that the syllable*
of their names mo-quauh-zo-ma should spell the word Moguauh-
zoiua (see Aubin's. introduction to Brasseur, Ilist. du, iUxiijue,
vol. L y. Ixviii.). > Tho anelogj- of this to the manner in which tho
Egyptian hieroglyphs passed into phonetic signs is remarkable,
and writing might have been invented anew in Mexico had it not
been for tho Spanish conquest. The Aztec numerals, which «ir«
vigesimal or reckoned by scores, were depicted by dots or cir les
up to 20, which was rem-cseiitcd by a flag, 400 (a score of scores)
by a feather, and 8000 (a score of scores of scores) by a purse ; bat
for convenience these symbols might be halved and quartered, so
that 534 might bo shown by one feather, one ijuarter of a feather,
ono flag, oue-half of a fljig, and four dots. The Jlexican calendar
depended on tho combination of numbers with pictiiro-signs, of
which the four principal were the rabbit, reed, flint, house —
tocJitli, acatl, iecpatl, calli. The cycle of 62 years was recltoned by
combining thoj^e signs in rotation with numbers up to 13, thus: —
1 rabbit, 2 reed, 3 (lint, 4 house, C rabbit, 6 reed, ic. liy accident
this calendar may be exactly illustrated with a modern pack of
cards laid out in rotation of the four suits, as, aco of hearts, £ of
spades, 3 of diamonds, 4 of clubs, 5 of hcti-ts, 6 of spades, &c. la
the Mexican ritual calendar of the days of the year, the same method,
is carried further, the series of twenty day-signs being combined
in rotation with numbers up to 13 ; as this cycle of days only
reaches 260, a series of nine other signs are aflixed in addition, to
make up the 365-day year. It is plain that this rotation of signs
8cr\'e<l no useful purpose whatever, being less convenient than
ordinary counting such as the Mexicans employed in their other
calendar already mentioned, where the 20-day periods had cacti a
name like our months, and their days had signs in regular order. It4
historical interest depends on its resemblance to the caleudar-systtnj
of central and eastern Asia, where among Alongols, Tibetaus,
Chinese, &c. , series of signs are thus 'combined to reckon years,
months, and days; for instance, tho Mongol cycle of 60 years ia
.recorded by the zodiac or series of 22 signs — mouse, bull, tiger, A:c.,
combined in rotation with tho five male and femalo elements — liro,
cartli, iron, water, wood; as " malo-fire-buU " year, kc. This
comparison is worked out in Iluniboldt's Vues 'des CordilUrea,
as evidence of Mexican civilization being borrowed from Asia.
Naturally tho Mexican calendar-system lent itself to magic in tho
same way as the similar zodiac-signs of tho Old World, each
person's fate being alfeoted by tho qualities of tho signs be waa
txirn under, an<l tlie astrologer-priests being called in to adriso on
every event of life. Of all Mexican festivals tho most solemn
was that of tho xinhmolpilli^ or " year-binding," when tho 62-
year cycle or buiullc of years came to an end. It was bolioved
that tho destruction of tho world, which after tho Hindu manuor
tho Mexicans held to have already taken place three or four times,
would happen again at tho end of a cycle. As the time drow
near, the ansious i>opulation chansed their houses and put out all
fire, and on tho last day after sunset the priests, dressed in tho garb
of gods, set out in procession for tho hill of Huixachtla, there to
wat<.h for tho ajiproach of the Pleiades to the zenith, which gavo
tho auspicious signal for tho lighting of Uie new firo. The finest
of the captives was thrown down and fire kindled on his breast by
tho wooden drill of the priest ; then iho victims heart was torn out,
and his body flung on tho pile kindh-d with the new flame. Tho
people watching from their flat housetops all tho country round
saw with joy the flamo on the sacnd hill, and hailed it with a
thank -offering of drops of blood drawn from their ears with sharp
stone-flakes. Swift runners carried burning brands to rekindle tho
fires of the land, tho sacred firo on the teocalli of tho war-god
blazed up again, and tho people began with feasting and rejoicing
the new cycle.
Mexican education, at any tato that of the upper class, was a Eduoa
systematic discipline much under the control ol religion, which tlon.
hero presents itself under a more favourable light. After tho
birth of a child, the tonalpouJiqiii or "sun-calculator" drew its
horoscope from tlie signs it was born under, and fixed tho time for
its solemn lustration or baptism, performed by the nurso with
appropriate prayers to the gods, when a toy shield and bow wore
provided if it was a boy, or a toy spindle and ilistalf if it was a girl,
and the child received its name. An interesting picturo-writing, to
be seen in Kingsborough, shows tho details of the boy's and girl's
iducation, from tho early time when three small circles overthe
child show it to bo three years old, and a drawing of half a tortilla
or corn-cake shows its allowance for each meal ; as they grow older
the lads are aeon beginning to carry burdens, paddlo the c&no^
and fish, while the girls learn to spin and weave, grind maize, and
cook,— good eonduet being enforced by nunisbments of increasing
severity, up to jiricking their bodies .vitli aloe thorns and holdina
MEXICO
213
iiiiliury interesu. Kor was the wealth and luxury of Mexico and Art wi^
surrounding regions without i correspondiii;; development of art. putimt
The stone sculptures sQchas that rAnainiiigof Xochi^-aU'o, which is
figured by Humboldt, as well as the oniamenUd woo<l«ork, feather-
mats, and vases, are not without artistic inejiL The often-cited
poems attributed to Nezahualcoyotl may not be ijuilc genuine, but
at any rate jtoetry had risen above the barbaric level, while tho
mention of ballads among the [icople, court odes, and the diants of
tcmplo choirs would indicate a vocal cultivation above iJiat of tlio
instrumental music of drums aud horns, piita and whistles, tlio
latter oftrn of pottery. Solemn and gay dances were frequent, and
a sport called tho birddaucc excited the admiration of foreigners
for the skill and daring with which grouiis of jicrformH-s dressed as
birds let themselves down by ro|>es wound round tho top of a high
mast, so as to fly whirled in arcles far above the ground. The
ball-game of tho Mexicans, called thi<htU, was, like tuiuLs, the \ai-
time of princes and nobles ; si>ecial courts weio built for it, and the
ball of india-rubber (pcrhajis the firet object in which Enroiwaus
became acquainted with this valuable material) might not be touched
by the hands, but was driven a^'aiiist the walls by blows of the knee
or elbow, shoulder or buttock. 'I'ho favourite game oCynlolli has beeii
already mentioned for its similarity to the yachUi of modem India.
The accounts given by Sjianish writers of the Central Americans Cestnl-
iii their stato after tho Sianish conquest are verj- scanty in com- Ameiicai
parison with the voluminous descriptions of Aztec life. Ihey bring cult««,
out iierfectly, however, the fact of close connexion betweeji Uie two
civilizations. Some Central-American p.oplcs «crc actually Jlcxicau
in their language and culture, csnecial'.y the PipiUof Cuatcmala and
a large part of tho jiopulation of iCiraragua, but tlicso were descend-
ants of Aztecs or allied i«oplcs who in the comparatively modern
times of Aztec power invaded and colonized tliesc distant countnes
(see Busdimann, AiUk. Ortsnai.ien, viii., ix.). With regard to the
Central-American nations proiwr, especially the Mayas of 'iucatan
and tho Quiches of Guatemala, who dwelt in tlio cities and wor-
shipped in the temples of Chichen-Itza and XJxmal, Falenque aud
Copan, the j.roblan of Aztec connexion is deeiier aud obscurer.
How closely related these nations were in institutions to the
Mexicans appears, not only in their using the same peculiar weaions,
such as the spear-thrower and tho toothed club or niaquahuill, but
in the similarity of their religious rites, such as drawing blood from
their bodies as an act of penance, aud sacrificing human victims by
cutting open tho breast and tearing out the heart; the connexior. is
evident in such special points as the ceremony of marriage by tying
together the garments of the couple, or in hohling an offender's face
over burning chillis as a punishment ; the native legends of Central
America make mention of the royal ball-play, which was the same
as the Mexican game of tJachtli already mentioned. At Uie same
time many of tlie Central-American customs dilTercd from the
Mexican ; thus in Yucatan we find the custom of the youths sleeping
;ho Europeans to prepare the beverage chccollall ; in a great bachelor's house, an arrangement common in variou,
passed iito Englfsh 'as the words caSio, or cocoa, parta of tho worid. b»t not in Mexico ; the same "n^"'' 8,^1.^ to
ervecoUbles adopted from Mexico are the tomata I the Maya cxogamo.is law of a man not taking a OTfo of !»' o"=
family name (see Diego do Landa, Hdacton tit i itcatan, ed.
lirasseur de Bourbourg, p. 140), which does not corie^iwnd with
Mexican custom. We have the means of com|wring the i*i-sona^
ppearance of the Mexicans and Central Americans by tlicir jior-,
their faces oTer burning chillis. The schools were extensive build-
ines attached to the temples, whore from an early age boys and
L'irls were tau"lit by the pnests to sweep the sanctuaries and keep up
the sacred fires, to fast at proper seasons and draw blood for penance,
and where theyreceived moral teaching in long aud verbose formulas.
Those fit for a soldier's life were trained to the use of wcajKins
and sent early to leani tho hardships of war ; chUdrcn of crafuinen
were usually Uught by their fathers to follow their trade; and for
the children of nobles there was elaborate instruction in history,
M ■ licturewriting, astrology, religious doctrines, and laws. Marriages
i^iia ,ler«ndcd much, as Ihcy do still in tho East, on comparison of the
horoscopes of tho [wir to ascertain if their birth-signs were com-
patible. Old women wore employed as go-betweens, aud the
marri.ige ceremony was conducted by a priest who after moral
exhortations united tho young couplo by tying their gatnicnU
to-ctli«r in a knot, after which they walked seven times round the
hi" casting inc^nso into it ; afUr tho performance of the mamage
ceremony tho pair entered together on a, four days' fast and
^'jaerals. penance before the marriage was comideted. The funeral rites
of the Mexicans arc best seen in tho ceremonies at the death of a
king. The corpse.laid out in state was provided by the priest with
a jug of water for liis journey, and with bunches of cut I>ai>er3 to
pri-< him safely through each danger of the road— the place where
th.; two mountains strike together, the road guarded by the great
sinko and tho great alligator, tho eight deserts and tho eight
hills; they gave him garments to protect him from the cutting
wind, and buried a little dog by his side to carry him across the
nine waters. Then the royal body was invested in the mantles of
his latrongods, esi)ccially that of tho war-god, for Mexican kings
were warriors ; on his faco was placed a mask of turquoise mosaic,
and a green ehalchihuitostono as a heart between his lips. In older
times tho dead king was buried on a throne with his property and
(lead attendants round him. But after cremation camo in a
mourning procession of servants and chiefs carried the body to the
funeral pyre to be burnt by tho demon-dressed priests, after which
the crowd of wives and slaves were exhorted to serve their lord
faithfully in tho next world, were sacrificed and their bodies burnt
Common people would not thus be provided with a ghostly retinue,
but their simpler funeral ceremonies were as far as they went similar
to those of their monarch.
Agricul- The staple food of the Mexicans before the conquest has continued
l«f» and with comparatively little change among the native race, and has
■ttti.1 even been adopted by thoso of European blood. Maize or Indian
corn was cultivated on patches of ground where, as in the Hindu
jliiii, the trees and bushes were burnt aud the seed planted in the
■oil manured by the ashes. A sharp-iwinted planting stick, a
wooden shovel, and a bronzo-bladcd boo called a coatl were tho
eimplc implements. The Mexicans understood digging channels
for irrigation, especially for tho cultivation of the cacahuatl, from
ivhich they taught tho Europeans to prepare the beverage chocollall;
these native names passed intoEngli: ' '' -
and chocolate. Other vegetables adop
{tomatl) aud the chUli, used as flavouring to native dishes. Th
inaize was ground with a stone roller on the grinding stone or nutlatl,
still known over Spanish America as the mdale, and the meal baked
into thin oval cakes called by Aztecs tUxcaUi, and by Spaniards
by tapping tho great'aloe before flowe"ring was fermented into in Central America to an extent quite beyond any such habit in
"1 'r"ii".'» \ t; , .,'•,, __ ..,,.■ 1... .1.. Mexico. It is from the ruined cities now buiicU in the l,eiilral-
an intoxicating drink about tho strength of beer, iKtli, by the
Pothing S|«iniards called putqut. Tobacco, smoked in loaves or canc-pipcs
<l or taken as snuff, was in use, especially at feasts. It is related that
in old times Mexican clothing was of skins or woven aloe and palm
kents. fibre, but at the time of the Conquest cotton was largely cultivated has no so Ud evidence ; some of th m ""^ ''"« ^'"""'^^Vv^?,
■n the hot lands, spun with a spindle, aud woven in a rudimentary doned before ho conquest, but °'"'^" J"? ■"' "^''^J, "'',°? %
loom without aslmttle into tile inaitles and breechcloths of tho ancestors of the Indians '^Ijo.now build their mean huts and D
American forests that we gain the best infonnatioM as to the nations
built them. The notion sometimes proiwundcil that these
famous cities were of great antiquity and the work of extinct nations
■ em may have been alioady aban-
thcra were inhabited, and by the
I and skirts of the women, garments otnn of I their patches of
MeUI-
Inrlc
of a reed-blowpipe and cast them solid or- hollow, and were
iilso skilled in hammered work and chasing, as some fine specimens
remain to show, though the famous animals modelled with gold and
silver fur. feathers, aud scales have disappeared. Iron was not
known, but copper and tin ores were mined, and the metals com-
bined into bronze of much the same alloy as in the Old World, of
which hatchet blades and other instruments were mode, though
their use had not superseded that of obsidian and other sharp stone
flakes for cutting, shaWng, &c. iletals had passed into a currency
for trading purposes, csjiecially quills of gold-dust aud T-shaped
pieces of copper, while cocoa-beans furnished small change. The
vast size of the market-squares with their surrounding porticos, and
the importance of the caravans of merchants who traded with other
■atioDS, show that mercantile had risen into some proportion to
round the relics of the grander life of theii
ruins through the districts ol
Honduras, it is evident that,
e nation, but of two or more
nations had tho pi-cat bond
f'a common system of pictorial or written characters. One speci-
men of a Central-American inscription may give a general idea ol
them all, whether it be from the sculptured favade of a temple
sketched by Catherwood, or from the painted dcerekiu called the
Dresden Codex (reproduced in Kingsborough), or from tho chapter
of Diego de Landa where ho professes to explain and translate the
characters themselves. These consist of combiuatioiis of faces, circles,
lines, ic, arr.inged in compartmenU in so complex a manner tliat
hardly two arc found alike. How they conveyed their meaning,
how far they pictorially represented ideas or spelt words m the
different languages of the country, is a question not yet answered
in a complete way; Landa's description (p. ?20) gives a table of ■
number of their elemenU as phonetically representing letters ol
syllables, but, though there may be a partial truth in lus rules, the-
214
MEXICO
are too insufficient or too erroneous to serve for any general deciphci -
roent. Most of what has been written on this enticing subject is
worthless, but a promising attempt has been made by E. S. Holden,
who has analysed tlie combined figures into tlieir elementary lines
(First Annual Ecport of Bureau of Elhiwlogy, Smithsonian Insti-
tution, Washington, 1881 ; see aho Charencey, 'Melanges de Fhilologie-
et de PaUugraphie Americaines, Paris, 1883). One point as to the
Central-American characters is clear, that part of them are calendar-
sigTis recording dates. From the accounts given by Landa and other
writers it is plain that the Central-American calendar, recltoning
the year in twenty-eight periods cf thirteen days, was the same in
its principle of combining signs as that of Mexico hero mentioned
at page 212. The four leading Maya signs called kan, muhic, ix, cuuac
corresponded in their position to the four Aztec signs rabbit, reed,
flint, house, but the meanings of the Maya signs are, unlike the
Aztec, verj' obscure. A remarkable feature of the Central-American
ruins is the frequency of truncated pyramids built of hewn stone,
with flights of steps up to the temple built on the platform at top.
The resemblance of these structures to the old descriptions and pic-
tures of the Mexican teocallis is so striking that thi:) name is habitu-
ally given to them. The teocallis built by the Nahua or Mexican
nations have been mostly destroyed, but two remain at Huatusco
and Tusajian (figured in Bancroft, vol. iv. pp. 443, 45C), which bear
a strong resemblance to those of Palenque. On the whole it is not
too much to say that, in spite of differences in style, the best means
of judging what the temples and palaces of Mexico were like is to
>>€ gained from the actual ruins in Central America. On the other
hand, there are features in Central-American architecture which
scarcely appear in Mexican. Thus at Uxmal there stands on a
terraced mound the long narrow building known as the governor's
house (Casa del Gobemador), 322 feet long, 39 feet wide, 26 feet
high, built of rubble stone and mortar faced with square blocks of
etone, the interior of the chambers rising into a sloping roof formed
by courses-of stonework gradually overlapping in a "false arch.''
The same construction is seen in the buildings forming the sides of
a quadrangle and bearing the equally imaginary name of the
nunnery (Casa de Monjas); the resemblance of the interidr of one
of its apartments to an Etruscan tomb has often been noticed (see
Fergusson, History of Architecture, vol. i. ; VioUet-le-Duc, in
Charnay). Attempts to trace the architecture of Central America
to direct derivation from Old-World types have not been successful,
while on the other hand ilsdecorationshowsproofof original inven-
tion, especially in the imitations of woodwork which, as the above-
mentioned arcliitects have pointed out, passed into sculptured
ornament when the material of construction became stone instead
of wood. Thus the architectural remains, though they fail actually
to solve the historical problem of the high culture of the nations
round the Gulf of Mexico, throw much light on it when their
evidence is added to that of religion and customs. Whether Mexican
civilization was a barbaric copy of that which flourished in the now
deserted Central-American cities, or whether the nations who built
these cities themselves raised to a higher level a civilization derived
from Mexico, two things seem probable, — first, that the civilizations
of Mexico and Central America were pervaded by a common influence
in religion, art, and custom ; second, that this common element
shows traces of the importation of Asiatic ideas into America.
Among works of reference on tlie ancient history- and civilization of Mexico
and Central America may be mentioned H. B. Bancroft, T^e Native Races t(f the
Paxific States o/ North America, London, 1S75-6 (contjilns the most complete
Biimraary, witli references to original autlioritics) ; Brasgcur de Bourbourg,
Uistoire des Nations Civilise'es dtt Merioue et de I' Am^rique-Centrale. Parij,
1867-59 (a valuable coiiecUon of materials.'but the author's own views are mostly
fnncifu]); Prescott, History of the Conquest of Mexico; Clavlgero, Eloria Antica
tlel Mesttco, Cesena, 1780 {contains the substance of earlier writers, such as
Gomrra, Torqnemada, AcosCa, Bottu'lni, &c.). For special topics: — Lord Kings-
borough, Antiquities of Mexico, London, 1831^8 (contains facsimiles and Inter-
pretations of plctare-^vritings, the native chronicles of Ixtlllxochltl and Tciczo-
moc, a reprint of Sahagun Ac.); A. von Humboldt, Viies des Cordiltires, et
iionttmens des Peuples Indigenes de rAm&iqite, Paris. 1816 (Mexican civilization,
plctare-wrltlng, calendar, itc.). Travels and descriptions of antltfuitles, Ac: —
Dnpaix (in Klngsborongh) ; C, Ncbel. Viqje Pintoresco y Arqueoidgico sobre la
Rejnibtica Mtjteana, Paris. 1839; F. de Waldeck, Voyage Pittoresgue tt Arehifo-
togiqne dans la Province d Yucatan, Paris, 1838, and Palengu^ et Aulres Jiuines,
Paris, 1866 ; D. Charnay, Cites et Rutnts A mertcaines, avec textc par ^'loilet-le■Doc,
Paris, 1863; J. L. Stephens, Incidents oj Travel in Central America, Ac, Now
York, 1841; Incidents of Travel in Yucatan, New York, 18&8; Brantz Mayer,
Mexico, New York, 18M; Tylor, Anahuac, or Mexico and the Mexieani, London,
18«1. *c (E, B. T.)
II. THE REPUBLIC OF MEXICO.
Mexico, Aztec Mexitli ' (^stados Unidos de Mexico),
is' a federal republic in Noi th America, bounded N. by
the United States (California, Arizona, and New Mexico),
E. by Texas and the Gulf of Mexico, S. by Guatemala anil
* In this, asinallother AztecnanK . the a: terj) represents the English
soand sk; hence Mexitli and Mexi o should be properly pronounced
Mtskitli, Meskico. But they do nol appAr to have ever been so pro-
noonced by the Spaniards, who naturally gave to the x its ordinary
Bpanish soimd ol the Gtmian ch.
British Hondura-s, where the boundary lines are still partly
undetermined, W. by the Pacific Ocean. Lying between
33° and 15° N. lat. and 87° and 117° W. long., Mexico
stretches about 1950 miles in,rth-north-west and south-
Bouth-east, with a mean breadth of 400 miles, varying
from about 1000 in 26° N. to 130 at the narrowest
part of the Tehuantepec isthmus. It has a coast^line of
nearly 6000 miles, — about iSOO on the Pacific and 1600
on the Atlantic. The seaboard is little varied either
by deep inlets, bold headlands, broad estuaries, or large
islands. On the west side are the vast Gulf of California,
in outline somewhat resembling the Bed Sea, and so named
by some of the early navigators, and the open Bay of
Tehuantepec, besides the smaller inlets of Acapulco and
San Bias, forming two of the finest harbours in the world,
and almost the only safe ones in the republic. On tlie
east side the coast is mostly beset by lagoons and sand-
banks, with no good havens, Camp^che, Vera Cruz, Tampico,
and Matamoras being all little better than open roadsteads
exposed to the fierce " nortes," or north-easterly gales, that
sweep the Gulf of Mexico for a gTeat part of the year. Of
headlands the most prominent are Capes S. Lucas and
Palmas at the south e.\tremity of Lower Cahfornia, Oor-
rientes south from San Bias, and Catoche in the north-
east of Yucatan. Besides this peninsula, which projects
north-north-east, the only other 's that of Lower California,
which projects south-south-east parallel to the mainland.
The islands are few in number, and all of insignificant size,
the most noteworthy being Tiburon and Angel de la Quarda
in the Gulf of California, the uninhabited Eevillagigedo
group in the Pacific, and Cozumel off the Yucatan coast.
Mexico comprises altogether twenty -seven confederate
states, one territory, and the Federal District, with areas,
populations, and chief towns as under :'^ —
States.
Area in
Square
Miles.
Popula-
(18S0).
Capital.
Popula-
(1877-80).
E
1
<
t
Sonora
81,022
105,295
61,050
14,363
28,659
2r,«3
12,716
26,083
32,658
25,927
48,967
2,393
21,609
51.226
27.389
16,769
42,643
26,585
2,210
28,889
11,1.10
3,429
8,480
9,598
1,898
11,761
1,498
84
59,033
139,140
180,758
104,131
194,861
144,747
604,970
93,.'i87
86,299
286,384
167,093
994,900
65,827
648.857
308,716
718,194
219,735
190,846
413,6M
140,430
506,799
788,202
179,915
434,096
696.038
164,94«
704,372
133,498
8M,S40
23,196
9,700
12,116
11.340
16,300
■»,800
12,400
6,800
15,190
32,000
7,878
78,600
23,872
20,400
3,600
26,228
8,500
27.119
32,000
31,871
34,300
(6,113
27,660
12,500
12,700
16.320
64,588
4.300
241,110
2,396
Tamaullpas,
Cludad victoria ...
San Juan Ilaulltta.
/Slnaloa «
Culiacan
Colir.ia
Oajaca
Oajaca
San Cristobal
Durango
Agnaa Callentes.....
San LuisPotosi....
Guanajuato
Queietoro
Mexico
PoffLral''ni«('H'/-'t
Lower California )
(Tenltorj) f
La Paz
: 63,804
9,577,279
Since the appearance of A. von Humboldt's classic Pbydeat
work on ^ew Spain, as Mexico was called in the colonial featnrm.
times, this region has continued to be regarded as forming PlatMos
a main link in the vast chain supposed to stretch across "g^.
the entire length of the American continent from Cape ^^jj^
* These figures, in the ftl'sence of scientific surveys and a trust-
T^orlhy census, .ire necessarily more or less approximate. The areas
are those of Ripley and Dana, based on A. Garcia Cuba's Carta ffeo-
grafca (Mexico, 1874); the populations of the states and capitals ar»
the estimates cf 'Gniiliano Busto in his Estadistica -U la kepulHca
Mrxicana (Mexico, USU)- A writer iii the Time of December 7,
1882, estimate;! the whole population at 12,000,001/, much too high s
fieri re.
il E X
Horn to Behring's Strait. But more recent research, and
especially the surveys made by the French staff during the
military operations between 1S61-67,' have shown that
this grand generalization must be abandoned. In remote
geological epochs a marine channel seems to have flowed
between the northern and southern sections of the New
World at the isthmus of Panama, while Mexico itself
appears to be mainly a distinct geographical region
of relatively recent upheaval. Here there nowhere exists
a continuous mountain range, to which might properly be
applied the designation "Cordillera of the Andes," an
expression which in any case is not current north of the
isthmus of Tehuantepec. Mexico forms, on the contrary,
a vast tabl&-land, somewhat in the shape of a cornucopia,
\ritli its narrow end tapering to the south-south-cast, its
convex and concave sides facing the Pacific and Atlantic
respectively, and with a general inclination northwards.
Most of the so-called Cordilleras are merely the " cumbres "
or escarpments of this plateau, which falls abruptly towards
the Atlantic, and through a series of well-marked terraces
(formerly lacustrine basins) towards the Pacific. Thus the
carriage road from the capital runs in tolerably easy stages
successively through the Tetla (8000 feet), Mescala (5500),
Papagallo (1800), and Peregrino (IGOO) valleys down to
Tepes within 40 miles of the seaport of San Bias. But
the southern central plateau of Anahuac maintains its mean
elevation of 7000 to 8000 feet almost everywhere to within
35 or 40 miles of the Atlantic. Hence the railway opened
in 1872 between Vera Cruz and the capital has had to be
carried by tremendously steep gradients to a height of
nearly 8000 feet within a total distance of 263 miles."
The general but gradual northerly tUt of the table-land is
shown by the altitudes of the capital, Durango, Chihuahua,
and Paso del Norte on the United States frontier, which
are respectively 7600, 6630, 4600, and 3800 feet.
At the same time the scarps rise in many places con-
siderably above the mean level of the plateau, which is
itself intersected and broken into a number of secondary
valleys by several short cross ridges, generally following
the normal direction from north-north-west to south-south-
east. The most continuous range is the Sierra Madre of
the Pacific, which may be traced at a mean elevation of
over 10,000 feet from Oajaca to Arizona, and which from
Guadalajara to the northern frontier is crossed by no
carriage route. Parallel to this is the Lower CaJifomian
range (Sierra de la Giganta, 3000 feet), which, however,
falls abruptly eastwards, like the Atlantic escarpments.
The Califomian peninsula seems to have been detached
from the mainland when the general upheaval took place
which produced the va^t chasm now flooded by the Gulf
of California. Corresponding with the Sierra Madre of
the Pacific on the west are the more interrupted eastern
scarps of the central plateau, which sweep round the Gulf
of Mexico as the Sierras Madres of Nuevo-Leon and
Tamaulipas at an elevation of about 6000 feet. These are
crossed by the carriage routes from Tula to Tampico
(highest pass 4820 feet), from Saltillo to Monterey (3400),
and at several other points.
Of the central cross ridges the most important orogra^
phically and historically is the Cordillera de Aiiahnac,^
ICO
215
' The results of these surreys are embodied in the Carte du itexique,
scale 1 : 3,000,000, published at Paris in 1873.
' In the steepest parts the mean is 2-51 in 100, or 133J feet to the
mile. The eiact elevation of the capital above the sea at Yera Cruz
appears to be 7550 feet, or 80 more than Humboldt's estimate.
• The term AnahuaCy meaning in Aztec " near the water," seems to
bave been criginallj- restricted to the central lacustrine basin of
TenochtitlaQ. But when the Aztecs reached both oceans they extended
it to the Pacific coast between Tututepec and Guatemala (Anahuac-
(Ayotlan), and to the Atlantic coast between the Alvarado and
TabaKO rivers (Auahuac-Xicalanco). The original use of the word is
which surrounds the Mexican (Tenochtitlan) and Puebl.i
valleys, and which is supposed to culminate with Popo-
catepetl (17,853 feet) and Ixtaccihuatl (15,705).* But
these giants belong to a different or rather a more recent
system of igneous upheaval, nmning from sea to sea
between 18° 59' and 19° 12' N. in almost a straight line
east and west, consequently nearly at right angles to the
main axis of the central plateau. The line is clearly
marked by several extinct cones and by five active or
quiescent volcanoes, of which the highest is Popocatepetl,
lying south of the capital nearly midway between the
Pacific and Atlantic. East of this central point of the
system are Citlaltepetl, better known as the Peak of Orizalia
(17,176 feet), 70 miles inland, and San Martin or Tuitla
(9708 feet) on the coast south of Vera Cruz, to which
correspond on the west the recently upheaved Jorullo
(4000 feet) in Michoacan, Colima (12,800) near the coast
in Jalisco, and the volcanic EeviUagigedo group iu the
Pacific. South of this line, and nearly parallel, are the
Sierras of Guerrero, and south of the Tehuantepec isthmus
those of Oajaca and Soconusco towards the Gnateiuala
frontier. In the same direction run the islands of Cuba
and Hayti, which probably belong to the same Central-
American system.
Mexiijo is thus physically connected through its older
plateau formations with the North-American table-lands,
and through its more recent volcanic upheavals with the
Central-American igneous region. But as it advances
northwards this region loses in imderground energy ; hence,
notwithstanding the remarkable upheaval of Jorullo in
1759, the Mexican cones show little signs of activity,^ and
the land is now scarcely ever wasted by violent earth-
quakes. Such phenomena are most frequent in the Puebla
valley ; but, although often accompanied by the peculiar
underground rumblings known as hramidos, they are
seldom of a destructive character. The natives speak of
them rather as iemblores, or "tremblings," than true
ierremotos.''
In a region where lofty ranges and plateau forma- Hydro,
tions with steep escarpments approach almost everywhere grapby
to within a few miles of the coast, little space is left for
the development of large river basins. Most of the
streams are little more than mountain torrents rushing
impetuously from terrace to terrace seawards. Many also
still current amongst the natives as practicilly synonymous wth
Centi-al Mexico. As a strictly geographical expression it is vaguely
and often incorrectly used by modem writers.
* This elevation is based on the calculations of Humboldt, Glennie,
and Gerolt ; but in 1857 S^nntag assigned' an extreme height of over
17,000 feet to the highest peak of Ixtaccihuatl. Popocatepetl is usually
supposed to be the highest point of North America ; but the recent
United States surveys have transferred this honour to Slount Elias on
the Alaska coast, which appears to be certainly over 19,000 feet high.
' Popocatepetl emits smoke, whence its name, meaning in Aztec
"Smoking Mountain," irQmj)0})oca "to smoke," and tepell " moun-
tain." Since the conquest three eruptions have been reported (1519,
1539, 1540) ; but the geological evidence seems to indicate that
there has been no volcanic action for thousands of years. Orizaba,
whose native name means "Star Mountain," has been quiescent since
1566. Colima still frequently ejects ashes and smoke; but both
Jorullo and Tuxtla are quiescent, the last having been silent since the
violent eruption of March 2, 1793. Even the Mal-pays, or hot dis-
trict round Jorullo, has cooled down, and is now again clothed with
vegetation.
" It is notewortny that the seismic waves flow normally along ths
indicated line from east to west, thereby confirming Humboldt's view
that under about 19° N. there is a deep rent in the earth's crust,
through which at different periods the underground fires have broken
at various points between the Gulf of Mexico and the Revilla*
gigedo group. "Only on the supposition that these volcanoes, which
are on the surface connected by a skeleton of volcanic rocks, are also
united under the surface by a chain of volcanic elements in continual
activity, may we account for the earthquakes which in the direction
mentioned cause the American continent, from the Gulf of Mexico to
the Pacific Ocean, to oscillate at the same time " (Egloffistein, p. 37).
216
MEXICO
flow through the profound rocky gorges or barrancas, as
they are here called, which form a characteristic feature of
the Mexican table-lands.^ On the east side some of these
barrancas, here running mostly west and east, attain depths
of 800 to 1000 feet in "Ihe unfossiliferous limestones of
that region; and even on the west coast the De Beltran
canon is flanked by sheer rocky walls over 500 feet high.
Hence the rivers are almost useless for irrigation purposes,
and available as means of communicatioo only for short
distances in their lower reaches, where they flow through
the narrow alluvial strips of level coast-lands to the sea.
Even the Rio Grande del Norte, which is by far the
largest, and which forms the frontier line between Mexico
and Texas, is navigable by large vessels only for a few
miles above its port of Matamoras. The Eio Grande de
"Santiago, the largest on the Pacific side, is almost every-
where obstructed by falls and rupids. On this coast the
next in importance is the Mercala, or Eio de las Balsas,
which, like the Panuco, Alvaredo, Coatzacoalas, Grijalva,
and Usumacirita flowing to the Gulf of Mexico, is subject
to sudden freshets during the rains.
At this season the waters which find no seaward outlet
are collected in the depressions of the plateaus, where
extensive tracts remain flooded for several months at a
time. But these lacustrine basins of the Anahuac and
Chihuahua table-lands, standing at elevations of from 4000
to 7000 feet, are, by evaporation under semi-tropical suns,
rapidly reduced to their normal level. The diminished
size of the Anahuac lakes shows that since the conquest a
steady process of desiccation has been going on, due prob-
ably to the reckless destruction of the upland forests by
the European settlers. None • of these lakes are of great
teize except Lake Chapala, which is traversed by the Rio
Grande de Santiago, and has a reputed area of about 1300
square miles. Amongst those of the plateau especially
noteworthy for their magnificent scenery are Tezcuco and
Chalco, in whose sparkling waters are reflected the sur-
rounding volcanic peaks and extinct craters of the Anahuac
table-land, with a background formed by the Cordilleras,
whose snowy summits rise here and there high above the
dark pine forests of the lower slopes.
In the higher ranges the prevailing formations are
granites, which seem also to form the foundation of the
BJnarals. plateaus, above which rise the traps, basalts, mineral-
bearing porphyries, and more recent lavas. Hence LyeU'^
theory that Mexico consisted originally of granitic ranges
with intervening valleys subsequently filled up to the level
of the plateaus by subterranean eruptions. Igneous rocks
of every geologic epoch certainly to a large extent form the
superstructure of the central plateau. But the Mexican
table-land seems to consist mainly of metamorpldc forma-
tions, which have been partly upiheaved, partly inter-
penetrated and overlaid by igneous masses of all epochs,
and which are chiefly represented by shales, grejrwacke,
greenstones, silioious schists, and especially unfossihferous
limestone. All these formations are alike remarkable for
the abundance and variety of their metalliferous ores, such
as silver, silver-glance, copper, and gold. Gneiss and
micaceous schists prevail in Oajaca and on all the southern
slopes facing both oceans. But the highest ranges are
formed mainly of plutonic and volcanic rocks, such as
granites, syenites, diorites, mineral-bearing trachytes,
basalts, porphyries, obsidian, pearlstone, sulphur, pumice,
lavas, tufa, and other recent volcanic discharges. Obsidian
(ilztli) was the chief material formerly used by the natives
' " Near tlie niouritaia ranges, from which the water after heavy
raina rusliea do\vn in ianumerablo forest stream.^, these ravines are
ftlled with incredible rapidity as hifih as 80 feet,— the torrent importing
(ric) trees and bearing away rockj with a thimdering noise and
'nosistiblo power " (Egiolfetein, p. 22).
in the manuiacture of their cutting implements, as shown
by the quarries of the Cerro d^ las Navajas (" Knife Cliff ")
near Zimapan. Vast deposits of pumice and the purest
sulphur are found at Huichapa and in many of the craters.'
But immeasurably the most valuaVjle rocks are the
argentiferous porphyries and schists of the central plateau
and in Sinaloa, unless they are destined to be rivalled by the
auriferous deposits of Sonora.^ Horizontal and stratified
rocks, of extremely limited extent in the south, are largely
developed in the northern states, and chalk becomes very
prevalent towards the Rio Grande and Eio Gila valleys.
To this chalk and to the sandstones are probably to be
referred the sandy plains which cover vast tracts in North
Mexico, stretching thence far into New Mexico and Texas.
Here the Bolson de Mapimi, a vast rocky wilderness
inhabited. only by wild tribes, occupies a space of perhaps
50,000 square miles in Coahuila and parts of the surround-
ing states.
None of the horizontal layers seem to be very rich in
ores, which are found mainly in the metamorphic, palaeozoic,
and hypogene rocks of Durango, Chihuahua, and the south.
Apart from Sinaloa and Sonora, which are now known to
contain vast stores of the precious metalf, nearly all the
historical mines lie on the south central plateau at eleva-
tions of from 5500 to 9500 feet. A line drawn from
the capital to Guanajuato, and thence northwards to
the mining tovra of Guadalupe y Calvo in Chihuahua,
and southwards to Oajaca, thus cutting the main axis
of upheaval at an angle of 45°, will intersect probably the
richest known argentiferous region in the whole world.
The central group of mines in the three mineral districts
of Guanajuato, Zacatecas, and Catorze (San Luis Potosi),
which have yielded more than half of all the silver hitherto
found in Mexico, lie between 21° and 24° 30' N., within an
area of about 13,000 square miles. Here the Veta Madre
lode of Guanajuato alone produced .£504,000 between
1556 and 1803, besides £10,000 of gold. This metal,
however, occurs chiefly, not on the plateau in association
with sUver, but on the slopes facing the Pacific, and
apparently in greatest abundance in Sonora, near the
auriferous region of New California. In recent times over
half of the silver produced in the whole world has been
supplied by Mexico, and the total yield of the precious
metals between 1537 and 1880 was as under :' —
Gold.
SUver.
Total.
1537 to 1821
1821 to 1880
Total . ...
£14,000,000
• 10,000,000
£418,000,000
180,000,000
£432,000,000
190,000,000
£21,000,000
£598,000,000
£622,000,000
Of other minerals the most important are copper, found
in a pure state near the city of Guanajuato, and' associ-
ated with gold in Chihuahua, Sonora, Guerrero, Jalisco,
2 On the general character and distribution of the igneons formation*
Von Egloflstein remarks: "Intimate relations exist between the
metalliferous and non-metalliferous rorphyriesi. The metalliferous por-
phyry is less frequent, but constitutes the most important formation,
bearing the precious metals, . . . embr,wing the rich lodes of Real-del-
Monte, Pachuca, Chico, Capula, and Santa Rosa, all of great richness
and magnitude. They further form the mineral districts of Augan-
gnco, Oro, Iliiautla, &c., and part of the mountains of Zimapan and
Istapa-delOro. The lodes found in this porphyry are charactcriied
by their magnitude and the consisti'ncy of the ores they contain. . . .
The richest ores of native silver and sulpliurct, chloride, and oiido of
silver are found in the lodes of Rcaldel-Monte, Pachuca, and S«nt«
Rosa. . . . The gold seems to exist in small particles in the met»-
moqihic porphyry mountains, whence it is carrieii by the nuns to the
vallovs as the locks become disintegrated " (pp. 0-8).
> Time^ correspondent, December 7, 1882. Guanajuato seems to be
still the greatest producer, yielding from £1,500,000 to £1,750 000
yearly, although the grtat Valcnciana mine is Hoodod, anil of tho han-
dred opened only fifty-two am now worked (Geigcr).
[ICO
MEXICO
21T
Miohoacan, and elsewhere; iron in immense masses in
Michoacan and Jalisco, and in Duiango, where the Cerro
del Mercado is a solid mountain of -magnetic iron ore ; lead
associated with silrer, especially in Oajaca; tin in
Michoacan and Jalisco ; sulphur in many craters ; platinum
recently found in Tlaxcala and Hidalgo; cinnabar al»o
rtcently in Morelos and Guerrero ; " steppe salt " in the
sandy districts of the north; "bitter salt" at Tepeyac;
coal in limited quantities at various points ; bismuth in
many parts; marble, alabaster, gypsum, and rock-salt in
great abundance throughout the plateau and the sierras. In
1882 there were open altogether 569 mines : — 541 silver,
14 gold, 4 copper, 4 lead, 3 salt, 2 coal, and 1 mercury.^
mHiB Intersected about midway by the Tropic of Cancer,
*,"*^ and stretching across seventeen parallels of latitude,
Mexico, from its position alone, necessarily enjoys a great
diversity of climate. But from its peculiar configuration
this feature is affected far more by the relief of the land
than by its distance from pole or equator. This is especi-
ally true of the more fertile and populous section lying
within the torrid zone, where three distinct climatic regions
are distinguished, not according to their horizontal, but
according to their vertical position. The temperature
falling steadily with the elevation of the land, which here
rises rapidly from sea-level to nearly 18,000 feet above
the surrounding waters, the low-lying coast-lands, up to
about 3000 feet on the scarps and terraces of the central
plateau, are comprised within the first zone of tierras
calientes, or "hot lands." Within this zone are included
all the sandy and marshy tracts fringing the Gulf of
Mexico, the lower slopes facing eastwards and exposed to
the hot and moist winds from the Caribbean Sea, and most
of Yucatan and the Tehuantopee isthmus, besides the
narrow strip between the uplands and the Pacific which
broadens northwards along the east side of the Gulf of
California. Here the mean temperature varies from 77°
to 82° Fahr., seldom falling below 60°, but often rising to
105°, and in the sultry districts of Vera Cruz and Acapulco
to 110°. The extreme north-western parts of this region
come almost withLu the rainless zone, and the Califomian
peninsula itself- is subject to excessive droughts, rendering
it almost uninhabitable. But farther south the climate
on both seaboards may be described as humid, hot, and
extremely unhealthy, especially for Europeans. Yellow
fever and black vomit are here endemic. But these
scourges are at least compensated by a magnificent tropical
vegetation and extensive virgin forests abounding in
valuable timbers, dyewoods, and medicinal and other
useful plants. Of the 114 species of trees and cabinet
woods, 17 of oil-bearing plants, and over 60 of medicinal
plants and dyewoods indigenous to Mexico, and often
differing specifically from kindred varieties in Central
and South America, by far the larger part are repre-
sented in the tierras calientes. Amongst the most im-
portant of these forest plants are mahogany, rosewood,
• Loreozo Castro, MtxUo in 1882. According to this anthority tho
total yield ef the Mexican mines between 1637 and 1880 was
£776,278,000, while another estimate based on a report of the
Mexican mint gives it at £930,786,000. Of this a large amount has
been coined in Mexico, where there were eleven mints at work in 1876,
with a total annual yield of about £5,000,000. The total coinage
Bince the conquest has been estimated as high as £600,000,000, not
more than 5 per cent of this being gold. With regard to coal, the ex-
istence of which in Mexico has been recently denied by Mr Bigelowin
Sarper'i Magazine, official returns for 1882 give a list of over twenty
places where it has been found, though nowhere as yet in large quan-
tities. Petroleum also appears to be very abundant in several
localities. Amongst other natural products mention should be made
of amber, found on the Yucatan coast Mineral springs are very
namerous everywhere on the plateaus and terrace-lands. The most
famous are El PeCon and N. SeSora de Gnadelupe near the capital,
and Aguas Calientes farther north.
io— 10*
copal, caucho (india-rubber), jalap, sarsaparilla, and vanilla
Here also maize, supplying the staple food of the people,
yields prodigious returns, multiplying froin two hundred
to four hundred fold, and affording two, three, and even
four successive crops within the year. Rice, indigo, c6tto«i,
tobacco, and coffee all thrive well, while sugar, cocoa, the
banana, and several varieties of beans are largely cultivated.
The tobacco of Vera Cruz and Tabasco, the coffee of Colima,
and the cocoa of Oajaca and Chiapas are of unrivalled
excellence.
To the "hot lands" succeed in vertical position the
tierrax templadas, or "temperate lands," which comprise
all the higher terraces and the central plateaus themselves
between about 3000 and 8000 feet. With a mean tempera-
ture of from 62° to 70° Fahr., and oscillating between
such moderate extremes as 60° and 86°, this region enjoys
one of the very finest climates on the globe. The Puebla
and Anahuac table-lands are described by enthusiastic
travellers as "terrestrial Edens," with a perennial spring
symbolized by the evergreen oak, cedars, and many
analogous plants, which here attain their greatest perfec-
tion. The transition from the lower zone is often very
gradual ; and, while epidemic fevers cease altogether at
altitudes of 2700 and 2800 feet, the tropical flora invades
many parts of the terrace lands, and even of the plateaus
to heights of 4000 and 5000 feet.^ A certain uniformity
is thus imparted to the Mexican landscape by the wide
lange of the maize, wheat, tobacco, vine, coffee, and other
plantations, as well as by the palms, evergreens, mango,
olive, orange, lemon, yucca, and an endless variety of the
cactus family, one species of which forms hedges 20 feet
high on the Anahuac uplands. The central zona is on the
whole drier than the southern lowlands, although the
scarps facing seawards are often wrapped in the fogs and
mists of the intercepted moisture-charged atmospheric
currents. The heaviest recorded rainfall (90 to 100 inches)
occurs in the healthy Huatusco district of Vera Cruz, at
an altitude of 4380 feet.
In the highest zone of tierrca frias, or " cold lands,"
embracing all the highlands from about 8000 feet upwards,
the rainfall is five times less than on the tierras templadas.
Hence snow rests throughout the year only on the four
most elevated peaks of Popocatepetl, Orizaba, Nevada de
Toluca (15,000 feet), and Ixtaccihuatl. Characteristic
both of the tierras frias and templadas is the maguey
{Agave mexicand), whose fruit is edible, and whose
fermented juice has from time unmemorial supplied the
famous pulque, or national beverage of the Mexicans.
From the fibre of the heniquen, an allied species, is pro-
duced the " Sisal hemp " of commerce, which has in recent
years become the staple export of Yucatan.
Speaking generally, the four seasons are clearly marked
north of 28° N. lat. only. South of that parallel they
merge in the estacion de las aguas, or rainy season, from
May to October, and the estacion seca, or dry season, which
prevails for the rest of the year. The rains generally
begin on the east coast, gradually moving westwards. In
the Pacific the moist atmospheric currents are deflected
northwards, whence the striking contrast between the
2 On the Amilpas plateau, which stretches south of Popocatepetl at
a mean height of 5000 to 5400 feet, " coffee, sugar, and indigo ai-e culti-
vated, and most of the tropical fruits grow luxuriantly " (Egloffstein,
p. 17). Tho same authority gives the limits of vegetation in this
region at 12,614 feet, and the snow.line at 14,960 feet. He observea
that " nothing is more surprising to the traveller than the varieties of
climate under this zone, which vary according to the different elevations
above the sea. In a few hours we descended from the cold regions of
the fir and the oak, on the heights of Ozumba, to a hot climate, tierra
calicnte, where we found the most luxuriant vegetation, passing ia
that short time through successive changes of the most diversified
species of trees, plants, birds, insects " (p. 22).
21«
MEXICO
wooded filopeb of Briti^ Coltunbia and the treeless crests
of the arid Lower Califomian peninsiila.
Fauna. In ita fauna no less than in its flora Mexico fonns
a land of tranaition between North a,nd Central America.
In coDimon with the north it has several Tarieties of the
bear, the ivolf,- coyote, skunk, bison, squirrel, beaver,
marten, otter, rattlesnake, heloderm,^ mocking-bird, and
many wild fowl ; while its monkeys (five species), puma,
jaguar, ocelot, sloth, tapir, alligators (two species), iguana,
boa, scorpions, tarantulas, and numerous brilliantly coloured
naiTots, trogona, and humming-birds connect it with the
routhem regions. Peculiar to Mexico, and distinguishing
il. from most tropical and subtropical- lands, are its song-
•^ters, of which, besides the mocking-bird (zeuzontl), as
many as twenty species have been enumerated. The
coasts are well supplied ■with fish and turtles, while the
pearl fisheries of the Gulf of California continue to be a
source of wealth to that otberwiae unproductive territory,
yielding in 1875 pearls to the value of iil6,000, and
£28,000 worth of shells. All the European domestic
animals thrive well, and vast herds of cattle, horses, and
<»heep are found on the well-stocked ranchos of the
northern states. Hore some of the more prosperous
breeders own from twenty to thirty thousand head of
oxen, and next to the precious metals hides and cattle
are among the chief -articles of export.
Agricul- ^^^ i^ t^® south stock-breeding yields everywhere to
ture. agriculture as the chief occupation of the people. Being
largely volcanic, the soil Is here extremj^y fertile wherever
water can be had in sufficient quantities for irrigation
purposes. Next to mai^e, which with beans and chilli
forms the almost exclusive food of the Indians, the most
important crop is probably sugar, of which over 60 million
pounds are annually produced in the state of Morelos alone.
Coffee is extensively cultivated on the lower slopes, and
now exported in considerable quantities, especially to the
United States. The tobacco and cotton crops are yearly
increasing in importance, while from the maguey Ls
extracted, besides pulque, a spirit called mezcal to the
annual valufe of about £750,000, The aborigines are
partly employed as free labourers on the plantations, and
partly hold small plots liable to a light Government
tax. The food crops thus raised were valued in 1873
at £14,500,000, the agricultural produce at £30,000,000,
and the landed property at £85,000,000, but the last
item was estimated by the minister of finance at fully
, three times that sum, Tho value of arable freehold land
was .stated in 1882 to be from £1 to £3 per acre, accord-
ing to its proximity to or remoteness from rivers.
Indua- Of the industries strictly so called, those directly connected with
tries. agricultural interests have alone acquiied any considerable develop-
ment. Such are sugar refining, carried on on a vast scale, especi-
ally in Moroloa ; brev/iiig and distilling, chiefly from maguey; paper-
mikinff from various pulps and fibres ; grist-mills and saw-mills,
especially in Puebla, Queretaro, Guadalajara, and SaltiUo. A fevr
iron foundries have been at work for some years, and stout hand-
woven cotton and woollen fabrics are produced in many of the largo
towns. The rebozos (shawls) of Leon and Salvaticrra have a wide
repute, while Texcoco and Puebla are noted for their porcelain and
glass-ware. Among the petty industries are clay and rag jSgures,
artificial flowers, wooden toys, and gold filigree work, in the produc-
tion of which tho natives often display remarkable taste and skill.
Trade. But all these manufactured warns are solely intended to supply
tho local wants, so that the exports have hitherto been restricted
almost exclusively to the produce of the land and of the mines.
Of the former the chief items are coffee, Sisal hemp, tobacco,
hides, lumber, cochineal, indigo, and other dyes, Barsaparilla,
vanilla, orchil, india-rubber. But the precious metals still continue
to constitute fully two-thirds of all tho exports, which in 1882 had
a total estimated value of about i,'G,*O0,OOO. In the same year an
^ A specimen of tliis curious creature, tbo only known venomous
lizard (Ileloderma suspeciicm), reached the London Zoological Gardens'in
1882; its habitat is the north of Mexico, and New Mexico, ArL2ona,
and Texas.
equal sum represented tbo imports, the lesdinff items of which were
cotton, linen, liilk, and woolhii goods, metals, nardware, machinery,
nnd provijiona. Althorgh diplomatic and conaular relations with
Great BrilaJn have been suspended since 1867, that country still
continues to enjoy by far the largest share of the foreign trade,
taking about £2, 000, 000, of tho exports, and sending in return
about two-thirds of all the imports, 'for 1882. Next in importance,
in descending order, is the trade with the United States, France,
Gennaiiy, Spain, and Columbia.
Probably four-fifths of the exclianges now pass through Vera
Cruz, which, since tho opening of the railway to the Anahuac
plateau, has become tho natural out-port of the capital and all the
central states. It ia connected by several lines of o.:ean steamers
with Liverpool, Southampton, St Nazaire, and the Atlantic States
Of North America. On the Pacific seaboard, where the trade ia
largely in German hands, Acapulco and the other ports also enjoy
regular steam communication with San Francis;.o and Panama. No
accurate returns are available of the shipping ; but the yearly
arrivals in all the Mexican ports are stated to arer?.gp about five
thousand, — not more than one-fifth under the national flag.
Till recently the means of iutemal locomotion were mainly Corn-
limited to the wretched bridle-paths from the central plateau over nionica-'
the sierras and terrace-lands down to a few points on both coasts, tion.
and to twenty-four regular lines of diligences under one manage-
ment. But since the completion of the lino from Vera Cru2 to tlie
capital, with a branch to Puebla, tho Mexican railway system has
acquired a considerable development. The Intcr-Oceanic line across
the Tehuantepec isthmus ia in progress ; the Great Central Trunk
line running northwar'l.i through Chihuahua ^iU ero lon^ effect a
junction with the North- Americm net-work; and at the end of 1S82
there l^ad been opened tff traflSc altogether 2219 mi'i'^s. For that
year the number of passengers carried wi^ 8,250,CC0, and of mer-
chandisa 27J million tons, with net earnings £C40,000, or ^CSOO per
mile. Still more developed is the telegraph system, which is now
extended to all the state capitals, and through the Mexico-Mata-
moras line to ihe United States and the rest of the world. The
8150 miles open in 1SS2 forwarded 750,000 messages, or in the
proportion of 8 per 100 inhabitants.
For tho aaniQ year the estimated revenue was' £6,140,000, nniuu^
and expenditure £6,300,000. The foreign debt is stated to be
£19,600;000, and the internal about £10,000,000, or altogether at
the rate of £3 per head of the population. Most of the foreign
debt is owned in England, but tne British claims had long been
practically repudiated by the Mexican Government. At the end of
1882, however, a semi-official suggestion was made that a settle-
ment might be effected by Mexico paving 1 per cent, on the
capital for the first ten years, 2 for the second, and 3 there-
after, the whole sum, amounting to £16,000,000, to bo liquidated
in fifty years.- The revenue is chiefly derived from the customs,
and about £1,750,000 of the expenditure is absorbed by the army,
the peace footing of which is 22,500 men of all arms. Beyond a
few coastguard steamers maintained mainly for revenue purposes^
there is no navy. An indication of finan-.ial improTement ia
afl*orded by the establishment in 1882 of the Mixxan National Bahk
by a French company with a capital of £4,000,000. This bank is
jirivileged to issue paper money'up to £12,000,000, in i-etum allow-
ing the supreme executive to overdraw their account up to
£2,000,000. A further symptom of revival is presented by the
increasing business of the general post-office, which in 1880
forwarded 4,406,000 letters and packages through 873 offices.
Education also has made marked progress sinco the finwl £.!aca-
separation of church and state in 1S57. In that year the old ti jil
university of Mexico, a purely ecclesiastical institution alter tho
model of Ssdamanca and the Soroonne, was abolished, or rather waa re-
placed by special schools of law, medicine, letters, agriculture,' mines,
sciences, fine arts, and commerce, and a military college. These,
as well as numerous lower schools, including two hundred in the
capital alone, are all maintained by the state, while national schools
are supported by public grants in all the largo towns, and higher
institutions in the capitals of tho several states. There are
in all nearly five thousand public schools, besides establishments
for the deaf and dumb, the olind, and juvenile delinquents, and
Eumi-rous charitable foundations maintained by voluntary contri-
butions.
Roman Catholicism, which und-'r the Spanish rulo w.aa alone BcligioD.
tolerated, continued after the separation to be the stato rvlimon
till 1857. Since then, while all cburehes enjoy equal protection,
none are officially recognized. The great majority of the Indim
fidehs, mestizoes, and credos still adhere at least outwardly to the
Koniau Church, which is administered by a hierarchy of three arch-
bishops (Mexico, Morelia, and GuadulajaraJ and twelve bishopa.
But by the organic laws of 1856 and 1859 all ecclesiastical estates,
at one time comprising over one-third of tho soil, were nationalized.
- This advance towardfl.A.«ettlemcnt was put forward in the Tv>o
Repvblict of December 6, 1832, a Mexican Journal which refleott'
the views of the Oovemmect on all matters of foreign policy.
MEXICO
219
the ngulof clergy suppressed, anJ their monasteries, together with
all otlicr suiierfluous ecclesiastical structures, appropriated by the
state. During .the last few years American Protestant missions
have claimed some partial success, and the so-called " Church of
Jesus," nn undenominational body of a somewhat original type,
has found a number of adherents, especially on the Anahuac table-
land. But the Indios bravos, or uncivilized abori^nes, everywhere
follow the old spirit worship, while the Christianity of the Fideles
is little more than a cloak for the continuous practice o^the former
Aztec hcatlienism. The pomp of the Roman ritual is supplemented
by the feasts of the national worship, and the Pagan deities of the*
old cult are still represented by the saints of the Roman calendar.*
Aduilnia- Mexico constitutes at present a confe'deration of
tratioDi states modelled on that of the North-American Union,
and administered according to the constitution of 1857 as
amended in 1873-74. By popular suffrage are chosen the '<
president, the unper house (fifty-two members), and the
supreme judiciary for four years, and the lower house (two
hundred and twenty-seven members) for two years. The
senate, abolished in 1853, was restored in 1874, and
the chief justice is m ojjicio vice-president. The federal
states, which are divided, into a number of administrative
districts, enjoy full autonomy in all local matters. The
several constitutions are modelled on that of the central
government, and like it comiirise three departments —
legislative, executive, and judicial. Each state is repre-
sented in the federal congress in the proportion of one
member for every 80,000 inhabitants, and in the federal
senate by two members elected by suffrage in the local
congress. All external affairs and questions of general
interest are reserved for the central government. The
constitution as now established thus represents in theory
the complete overthrow of mediaevalism, and the absolute
triumph of the new ideas which in the Old World are
still in so many places struggling for the ascendency.
Histoiv. It is this struggle between privilege and popular
Colonial rights that lends its human interest to the otherwise
period, monotonous record of unresisted oppression and ajiparently
aimless revolutions which characterize the early and the
later periods of Mexican history, from the overthrow of the
native rule down to the present day. The early or colonial
period covers exactly three hundred years, — from the death
in 1.521 uf Guatemozin, last of the Aztec emperors, to the
withdrawal of the last Spanish viceroy, Don Juan O'Donoju,
in 1821. During these three centuries the attitude of the
masses was one rather of sullen submission than of active
resistance to grinding oppression. By the Spanish Govern-
ment Mexico was looked on merely as a vast metalliferous
region, to be jealously guarded against foreign intrusion
and worked exclusively for the benefit of the crown. The
natives were evangelized chiefly for the purpose of being
employed as slaves above and below ground, and thus was
introduced from the West Indies the system of reparti-
mientos, or distribution of the aborigines on the plantations
and in the mines. But, while this system proved fatal to
the natives of Cuba and Hayti, where it had to be replaced
by negro labour, the hardier populations of the Anahuac
plateau successfully resisted its blighting influences. It
proved in fact more disastrous to the oppressor than to the
oppressed. In those days Spain was commonly compared
to a sieve, never the richer for all the boundless wealth
d^a^yn from the New World. But the aborigines derived
at least some advantage from contact and partial fusion
' On the general state of religion in Mexico Bates well remarks:—
"Theedncatcd classes conform lo the outward ceremonies and ordi-
nances of the cliurcli, while inwanlly believing little or nothing of its
dogmas. The lower grades of society are, on the other hand, steeped
in tlie most grovelling superstition, intensified by many traditional
Indian reminiscences. Tins section of the community yields a blind
obedience to the clergy, notwithstanding the severe laws with which
the Government has endeavoured to counteract the influence of the
priests. Even so recently as 1874 a genuine case of witch-burning
occaned in Ulexim."— Central America, p. 34.
with a people of superior culture. This fusion, which may
be regarded as the chief outcome of the colonial admini-
stration, has contributed to the formation of the present
exceedingly complex Mejdcau nationality, in which the
Indian continues to be the predominating element. Taking
the whole population at less than ten millions, its ethnical
distribution appears to be at present as under : —
1. Full-blood Indians T.l..... ;.'..' 5,000,000
2. Mestizoes (half-caste Indians and whites) ^V...... 8,000,000
3. Creoles (whites of Spanish descent).. „, 1,500,600
4. Gachupines' (Spaniards by birth) 50,000
5. Other Europeans and Americans -^ 100,000
6. Full-blood negroes 1^,000
7. Zambos or "Chinos" (Indo-Africans) 45,000
8. Mulattoes (Eurafricaus) 5,000
Under the Spanish administration, which was marked on
the surface by few stirring events, such as warlike expedi-
tions, civil strife, or serious internal troubles, Mexico, or
New Spain, formed a viceroyalty at one time stretching
from the isthmus of Panama to Vancouver's Island.
Antonio de Mendoza, appointed in 1535 after government
by audiencias had proved a signal failure, was the first of
sixty-four viceroys who ruled with almost autocratic power,
but scarcely any of whom has left a name in history. Don
Juan de Acuiia (1722-34) is mentioned as having been the
only native American among them, and Don Juan V. G.
Pacheco (1789-94) had at least the merit of betraying
some regard for the social welfare of his subjects. •. Under
him a regular police, the lighting and draining of towns,
and other municipal improvements were introduced.'
But down to the early years of the present century all
emoluments in church and state, most of the large planta-
tions, of the mines, and of the commerce of the country,
continued to be monopolized by the privileged gachupines,
whom the Creoles and mestizoes had already begun to regard
as aliens. Hence the first reactionary movements, stimulated
by Napoleon's deposition of King Ferdinand and arrest of
the viceroy Hurrigaray in 1808, were aimed rather against
odious class distinctions and the intolerable oppression of
these aliens than against the abstract rights of the Spanish
crown. The long smouldering spirit of discontent at last
broke into open revolt in 1810 at Guanajuato, under the
leadership of Don Miguel Hidalgo. After his defeat and
execution in 1811, the struggle was continued by Morelos,
who, like Hidalgo, was a priest, and shared his fate in
1815. But he had already called a national assembly at
Chilpanzinco, and by this body Klexican independence was'
for the first time proclaimed in 1813. A guerilla warfare
kept the national spirit aUve till a fresh stimulus was
given to it by the Spanish revolution of 1820. Under
the leadership of the " Liberator " Iturbide, Mexican inde-
pendence was again proclaimed on February 24, 1821, and
the same year the capital was surrendered by O'Donoju,
the last of the viceroys. But even after the revolt had
thus been crowned with success a change of personnel
rather than of system was contemplated ; nor was Iturbide
proclaimed emperor until the Mexican crown had been
declined by a royal prince of Spain.
Almost sinjultaneously with this event the republican Period of
standard had been raised by Santa Anna at Vera Cruz 'udepeni
(December 1822). Thus the nation had no sooner got rid "'°'"
of foreign rule than it became torn by internal dissension.
But henceforth the struggle is not so much against the
privileged classes as between Conservative and Liberal
principles, — the former represented chiefly by the church
and the superstitious populace, the latter by the more
enlightened but not less unscrupulous sections of the com-
munity. From both the Indios Bravos, that is, about a
third of the whole population, hold entirely aloof, and take
advantage of the public disorders to continue their aggres-
' From the Aztec Gatzopin, centaur; also known as Chapetona.
220
31 E X r c 0
sive warfare against all alike.' Events now follow in quick
succession, and as many as three hundred successful or
abortive revolutions arc recorded during the brief but
stormy life of Mexican national independence.^ But amid
the confusion of empires, republics, dictatorships, and
military usurpations, succeeding each other with bewilder-
ing rapidity, the thoughtful student will still detect a steady
progress towards the ultimate triumph of those Liberal
ideas which lie at the base of true national freedom. A
brief tabulated summary of the raore salient incidents in
this eventful struggle must here suffice : —
1821-23. Jlc.xicau indertndence acknowlejgej by Spain ; regency
under Iturbide, wlin (1822) is elected hereditary constitu-
tional emperor; in December Santa Anna proclaims tlie
republic in Vera Ciiiz.
1823-24. Provisional Govcrnmeut ; Iturbide abdicates ; exiled,
withdraws to London, but returning is shot (1824).
'824. First Liberal constitution,— "Acta Constitutiva de la Federa-
cion .Mexicana," then comprising nineteen states and five
territories; first president D. Felix Victoria, known as
•'Guadalupe Victoria."
■■ 628-30. Conte.sted presidencies of Pedraza, Guerrero, and Busta-
mente.
18o5. Reaction of the churcU party; constitution of 1824 abolislicd ;
the confederate states fused in a consolidated republic under
Santa Anna as president, but practically dictator.
1836. Te.vas refusing to submit secedes, defeatsaud captures Santa
Anna.
1837. Santa Anna returning resumes office.
1839. Oravo's brief presidency followed by much anarchy.
1841-44. Santa Anna's first dictatorship with two others.
1844. Constitution restored with Santa Anna president; banished
same year, he is succeeded by Canalizo.
1845. Herrera president; disastrous war with Lnitcd States to
recover Texas.
1846. Santa Anna again presidi
1848. Treaty of Guadalupe; California and New Mexico ceded to
United States.
1853. Santa Anna's second dictatorship; treatyofJIcsilla (negotiated
by Gadsden) ceding extensive territory to United States and
reducing Mexico to its [n-esent limits ; great financial embar-
rassment; "Plan of Ayutla"; flight of Santa Anna followed
by universal chaos.
1855. Provisional Government under President Comonfort.
1856 Constitutional convention; radical reforms; luiiture with
Spain.
1857. Libeijil constitution of March 11 ; suspended December 1;
iijiiionfort dictator ; the reaction sup poitcd by the church,
large part of the army, and all Conservatives ; opposed ut
VeraCruzby Vice-president Benito Juarez at the licadof tlw
1867-G9. VarioL-s pronunciamiintos by Santa Anna and others.
1871-72. Juarez president ; he dies in office July 1872 ; succeeded
by his secretary Lcrdo de Tejada.
1873-74. The Liberal constitution of 1857, whidi had been twice
suspended (1858-60 and 1863-67), is now largely amended,
and continues to be henceforth the erganic law of Jlexico. '
1876. Tejada succeeded by PorGrio Diaz.
1880. Manui;! Gonzalez, reigning president
Since 1869 tlie Liberal party lias succeeded in jireserving peace at
t home und abroad, while establisliing democj-atic institutions on a
firm basis. A. v. Hunibohlt's gloomy anticipations' Ijave not beea
realjzed, and for the first time in its chequered histoiy Mexico may
I look forward witli some confidence to a bright future. Tlie plagu'»
spot is the uncivilized Indian element. But witli boundless natural
i-csources at its disposal, a wise administration may hope to over-
come tliat difficulty, and gradually effect a complete fusion of the
antagonistic racial elements.
J. Frost, Ilittorti of Sttxieo and in Wan, »,.n aiMc
OiUaiis, IBbJ: T. tj. Drocklihuii.!. iftiiro TD-iau, I.oi
itexiro itt IS8?, New York. ISSJ; Aubcrtin. A i'li'jlit
1692; K. Uuslti, tMailiilUa Je la llrptiblira tt'j
Alamaii. Uittoria de Mexico, Mexico, tKJ9-.',2'
Rrroliieioaet, r«iL'. 1831!; E. K. II. von Illchthufi
Uepuhlik ilexito, Ut'ilin. I854-.'.r»; W. It. Presc
Mexico, New Voik. 1847; L. .Miililini.fnrJt, Sthild,
\,n. 1882 ;
0 Urxicr..
I lieiiehung civj Oeographie, Et/itio-iiaphie, unit Sfali.'lilt, II
■ ■r,c\,Uexlc
. L. Mom. irexic; y aul
poliliscfitn Zuiltiude der
ylory of tUe Comiuctt o/
/irp. Ml xico. bctondert
. 1844; A. r>.
Thlimmcl. Mexico vnd die ihxicaner itt t'lmiiichor, socitilrr, tittd polittscher lUtit
Ittittg, tiluneco. 1848; DiantJ Mayer, SSxico as ,1 iras and as il is. New York.
1844. .ind ifrxico, Atlec, Spattisli, attil litpuUicati, Ilanfoi.l, 18sn; F. W. ^on
' Et'toffsteln, Coiitt-ibutiotts to the Geology attd the Phyittcat Oeot}fapt,tj of itrxt:c,
No« York, IS04 ; J. C. Beltrami, Le Mexitjiie. Tai Is li-ao; Mailamr C. [CiildcronJ.
do la 1). Illarca]. li/e itt Mexico. Jtc. wUli prvf..co l.v W. 11. rasrnlt. Lone-:.
1R4.1; A. .M. Gilliam, Ttaccis over titf TaUe-ltttidt. attd Cottlillrtat v/ Mtxico, Piiii-
ntlclphlfl, IS4R: A. von IIunit^oMt. i\cs del Cofdil'ites tt ittotttitttcttttt itcs ptuplet
indi.ieites de I'Anientjitc, I'arh. IRIO, un<l Wtsiictt Utter dttt pttHtit-rlteit Zuftartd dts
Kittjiyreirhs Seu-Spattiett, TUMnccn, IsOy-n (rn-ncli'cil., Vaila, 1811); .MipueJ
Lcido de Tejada, Cotttetcio ixtrrior de Mexico detde la Cvttt/iitsia hasta kity,
Mesico. 1853; Jolin .MacKiTeor. i7o(t» o/ J/cj-iVo (toinmcicini lnillla.*c.), Londt-n.
184C; Analcs del Mittistcrio de foititttto, eoloniiaciott, iitdtistrta, y eoiiiercio d( 'o
Repvbttca Mfxieatia y reperlorio de itolieias eolire eieitcias, artrs, y estadittter.
il'irinnat y estl'attjefa, Mixico, IS.'il-.'ii; Mrtuoria sot/re el eslaito de la atjricutttir,:
y viduftria dt; la Hepublica, que la direccion general de estos latitat prtsettta t.'
1 Cobicrtio Stiprittto, .tc, Mexic.i. 1843-10; Don Mariano Galvii. Ittdttitrta Xtirionr.l.
J Mexico, ISli, and EUatuloor-jaiticode la Itrpitblira Mrriaitta. Jlixko, Ix-'iT; II. W.
^ Hates. Ceittral Attiefiea, ic, Willi cllinoloclcol appendls by A. II. Keanc. London,
1«78; .Purveys ol llic Fltnt-ll Corps Exlpvdllionnaltc ciiibodii-d in Ilic Cant du
Mexii/tie. Willi areoiiipunjiiiK inoiingrapli by M. NIn.t, Tarls, lf<73. Oilier larco
and more or Iiss Iriibtivoiliiy maps arc— A. G. Cuba. Carta Geoyrajira, >lcxico.
1^74 ; Tl.c l.ibrar,, Map of Mrxtro. Cliliaco, 1812; Ilunibniilt, Atltis l!^tjraplttt)iie
et i'ltitti(/tje dii llotjauinc dc la Koucetle Espa^tie, I'arls. 1811; Mapa de lus L'ltajrs
Vnidct de Mexico, i,-., publislicd by J. Dbliii-ntll. New Yolk. 1847; Urui!, Carle-
Paris, 182.'<; II. KlcptH, Jfrj-ifo. Ttroi.inni
lit y C. dc BclKhcs, Ciirta tjettrjjiotiica de lets
I'lo dc Mexico fottttada ivtire obsmaeiotitt
0, 1827; liic laiKo pliyvical and ecological
above-quoted work ; and a cuod ulief mBi>
geiitruU Jcs Ktn
^■Vn
» Xfcxiraifis,
Cali/oniitii, Wi-I
11(1 r,
M7; F. deGc
prtncipaUs distr
0» III
neralef del E*
ostron.. baromrt
V '
intra/., Mcxi
mnp-t iici'nniii;in\
"K V
on EKloffslcin'
In v. lUtzcl's Ju
sMrr
CO, Urcsluu, 1
111. TllE CITY OF MEXICO.
J , , „_„. „_ Mexico, the capita! formerly of the Aztec empire and of
'Pu^s," or advanced Liberals; the "War of Reform" the Spanish colony of New Spain, and now of the republic.
begin/, and lasts till 1860.
1858-59. In the capital Comonfort is deposed by Zuloaga, who
abdicates in favour of Miramon, general of the Conservative
forces ; but, declining the presidency, Miramon restores
Zuloaga ; British legation violated ; in Veia Cruz the
United States envoy MacI.ean arknowlcdges Juarez, who
introduces further Liberal measures.
1860. Capitulation of Guadalajara ; (liglit of Miramon from the
capital ; triumph of tlie Liberals.
1861. Triumphal entry of Juari!z into the capit.il ; further radical
reforms ; marriage declared a civil contract ; celibacy and
ecclesiastical tribunals sujipressi-d ; confiscation of cliurch
property valued at i.'75,O00,00O and over a third of the soil ;
final separation of church and state; Spain, France, and
England urge claims for lo.iscs of their subjects resident in
Mexico ; convention of London ; intervention of the allies,
who occupy Vera Cruz in December
1862. Engl.and anil Spain withdraw, their claims having been
settled by negotiation ; war continued by France.
state, and federal di.strict of Mexico, stands on the Anahuac
plateau, 7.^)'J4 feet above sea-level, 21 miles from the south-
west side of Lake Tezcuco (Texcoco), the lowest and largest
of six ba.'sins filling thedeepcst dcjiression in the hill-encircled
Mexican valley. Situated in 19" 25' 45" N. lat and 99° 7'
W. long., it i-i 173 miles by rail from Vera Cruz on the
Atlantic, 290 from Acapulcoon the Pacific, 285 from Oajaca,
80."! from Matamoro.i on tlie United States frontier. Mexico
is the large-it and finest city in Sllani.^h America, forming
a wjuare nearly 3 miles both \\ ays, and laid out with perfect
regularity, all its six hundred streets and lanes running at
right angles north to south and east to west, and covering
within the walls an area of about 10 .stpiare miles, with a
population (in 1880) of 230,000. Most of the inhabitants
are pure-lilood Indians or mestizoes; but the foreigners,
1863-64. The eajiital oceujiied by the French; Louis Napoleon ] cliiefly French, English, Germans, American.s.and Siianinrds,
monopolize nearly all the trade, and as capitftli.sts, liankers,
merchants, and dealers enjoy an influence out of all
[iroportion to their numbers. A large portion of the
natives arc mendicants or vagrant.^, and the distinctly
criminal clement (20,470 in 1878) is kejit in order by a
police force of 1 320 men ; yet in that year there were as
many as 5370 knife-altack.-> and 3250 robberies. The
' Consulted shortly before his death as to the future prospects of
Mexico, with which his name was so intimately associated, Humboldt
ventured to prophcBy that "die Vercinigten Staaten wcrdcu esansicb
reissen liad Uaun selbst zerfallen."
■sal fusion of the Latin races : oders tin
Mexican imperial crown to the Austrian arehduki- Ferdinand
^laximilian, who accepts, and arrives in June 1864.
1867. After diverse issues the Kieiali withdraw ; Maximilian,
abandoned to ^lis fate, is catitured and sliot at Queretnro
(June 19),
' In December 1882 a party of seventy-five Mexicans and Americans '
were massacred in the state of Chihuahua by a band of Bravos. I
' Between 1821 and 1868 the form of goveminent was changed ten '
times; over fifty persons succeeded each otlier as presidents, dictators, '
or emperors; both emperors were sliot, Iturbide in 1824, Maximilian
in 1 867, and according to some calculations tliere occurred at least three
hundred iirontcnciamientos. I
MEXICO
221
Lroad, well-pared, and gas-lit streets present a picturesque
appearance with their quaint two- and three-storied stone
houses gaUy painted in white, red, yellow, or green, and
terminating everywhere with a background of rugged
sierras or snowy peaks which, owing to the bright atmo-
sphere at this elevation, seera quite close, although really
30 or 40 miles distant. All the main thoroughfares con-
verge on the central Plaza de Armas (Plaza Mayor, or
Main Square), which covers 14 acres, and is tastefully laid
out with shady trees, garden plots, marble fountains, and
seats. Here also are grouped most of the public buildings,
towering above which is the cathedral, the largest and
mo.st sumptuous church in America, which faces the north
side of the plaza on the site of the great pyramidal teocalli
or temple of Huitzilopochtli, titular god of the Aztecs.
This edifice, which was founded in 1573 and finished in
1657, at a cost of £400,000 for the walls alone, forms a
Greek cross 426 feet long and 203 wide, with two great
naves and three aisles, twenty side -chapels, and a magnifi-
cent high altar supported by marble columns, and siu:-
rounded by a tumbago balustrade with sixty-two statues of
the same rich gold, silver, and copper alloy serving as
candelabra. The elaborately carved choir is also enclosed
by tumbago railings made in Macao, weighing 26 tons, and
valued at about £300,000. In the interior the Doric style
prevails, Renaissance in the exterior, which is adorned by a
fine dome and two open towers 218 feet high. At the foot
of the left tower is placed the famous calendar stone, the
most interesting relic of Aztec cultiu-e. The east side of
the plaza is occupied by the old viceregal residence, now
the National Palace, with 675 feet frontage, containing
most of the Government offices (ministerial, cabinet, treasury),
military haadquarters, archives, meteorological department
with observatory, and the spacious hall of ambassadors with
some remarkable paintings by Miranda and native artists.
North of the National Palace, and apparently forming
portions of it, are the post-office and the national museum of
natural history and antiquities, with a priceless collection
of Mexican remains. Close to the cathedral stands the
Monte de Piedad, or national pawnshop, a useful institu-
tion, endowed in 1744 byTerreros vs-ith £75,000, and now
possessing nearly £2,000,000 of accumulated funds.
Facing the cathedral is the Palacio Municipal (city hall),
252 feet by 122, rebuilt in 1792 at a cost of £30,000, and
containing the city and district offices, the corporation jail,
and the lonja, or merchants' exchange. Around the
Plaza San Domingo are grouped the convent of that
name, said to contain vast treasures buried within its walls,
the old inquisition, now the school of medicine, and the
custom-house. In the same neighbourhood are the chiu-ch
of the Jesuits and the school of arts, " an immense work-
shop, including iron and brass foundries, carriage and cart
mending, building and masonry, various branches of joinery
and upholstery work, and silk and cotton hand-weaving "
(Brocyehurst). Other noteworthy buildings are the
national picture gallery of San Carlos, the finest in
America, in which the Florentine and Flemish schools are
well represented, tCnd which contains the famous Las
Casas by Felix Parra ; the national library of St Augustine,
with over 100,000 volumes, numerous MSS., and many rare
old Spanish books; the mint, which since 1690 has
issued coinage, chiefly silver, to the amount of nearly
£400,000,000 ; the Iturbide hotel, formerly the residence
of the emperor Iturbide ; the Mineria, or school of mines,
with lecture-rooms, laboratories, rich mineralogical and
geological^ specimens, and a fossil horse 3 feet high of the
Pleistocene period. Owing to the spongy nature of the
Boil, the Mineria and many other structures Lave settled
' out of the perpendicular, thus often presenting irregular
Unes^and a rickety appearance. Among the twenty
scientific institutes mention should be miade of the Geogra-
phical and Statistical Society, whose meteorological depart-
ment issues charts and maps of unsurpassed excellence.
Besides the chief market south of the National Palace there are
three others, all well stocked with meat, fish, and especially
vegetables, fruits, and flowers grown mainly on the chinampas, or
floating gardens of Lakes Chalco and Xochimilco. These gardens,
which were far moVe numerous in the Aztec times, are formed by
placing layers of turf on the matted aquatic vegetable growths to a
height of 2 or 3 feet above the water, and securing them by long
willow poles driven through them to the bottom, where they take
root They form plots 100 to 200 feet long by 20 to 100 broad, and
are firm enough to support the huts of the cultivators. From the
still extant illuminated tribute-rolls it appears that the Aztec
rulers derived a large share of the taxes from these gardens, which
at that time also covered the brackish waters of Lake. Tezcuco.
Before 1860 half of the city consisted of churches, convents, and
other ecclesiastical structures, most of which have been sequestrated
and converted into libraries, stores, warehouses, and even stables,
or pulled down for civic improvements. Nevertheless there still
remain fourteen parish and thirty other churches, some of large size
with towers and domes, and their number has now been increased
by six Protestant churches including the Anglican cathedral in
San Francisco Street. This is the leading thoroughfare, and is
rivalled in splendour only by the new Cinco de Mayo Street niuning
from the National Theatre to the cathedral.
The city is supplied by two monumental aqueducts, from Chapul-
tepec and the south-west, with good water at the rate of 44 gallons
per day per inhabitant.
Its industries are varied but unimbortant, consisting chiefly of
gold and silver work, coarse glazed ana unglazcd pottery of peculiar
form and ornamentation, paper, ifeather-work remarkable for its taste
and beautiful designs, toys, rosaries, cruciflxes, religious pictures,
lace, and some weaving.
Mexico enjoys an equable climate, with a temperature varying from
70° to 50° F., but rendered unhealthy by the exhalations from the
lakes and the bad drainage. The death-rate in 1876 was 59 per
1000, and 45 in 1878, pneumonia being most fatal (12 per cent, of the
total). Standing at the lowest level of a lacustrine valley, 1400
square miles in extent, and completely encircled by hills with uo
natural outlet, the city has always been subject to floodings from
the overflow of the neighbouring freshwater Lakes Zumpaugo and
Xaltocan on the north and Xochimilco and Chalco on the south,
which, in the 17th century, laid the whole district under water in
1607, and again for five years from 1629 to 1634. To remedy the
evil the engineer Martinez began in 1607 the great cutting 13 railea
long through the Nochistongo hill in order to draw ofi' the
discharge of Lake Zumpango, the highest in the valley, to the river
Tola, a tributary of the Paimco, flowing to the Atlantic. This work,
which cost the lives of 70,000 natives, was completed in 1789 ; but the
result was not satisfactory, and the city is still often flooded.
The chief public promenades are the Alameda, planted with
stately beeches ; the Vega, skirted by the Vega Canal, and adorned
with the colossal bust of Guatemozin, the last of the Aztec em-
perors ; the Paseo de la Kiforma, a fine avenue 3 miles long running
south to the famous castle of Chapultepec, a place intimately asso-
ciated with the names both of Montezuma and Maximilian. The
present castle, erected in 1785 by the viceroy Galvez on the site ol
Montezuma's palace, commands a superb view of the city and siir*
rounding district, and is approached by avenues of gigantic
cypresses {Cupressu3 disticha) dating from A^tec times, growing to a
height of 120 feet, and measuring from 30 to 40 feet roimd the stem.
Other good roads with horse or steam trams lead to Tacubaya and
the " Noche Triste " tree, where Cortes is traditionally supposed to
have rested after the disastrous retreat from Mexico on the night of
June 30, 1520, to the pleasant summer suburb of Tacubaya, and to
the renowned shrine ot Our Lady of Guadalupe, 3 miles to the east on
the border of Lake Tezcuco. Here stands the most famous church
in Mexico, erected to commemorate the legendary apparitions of the
Madonna to the Indian Juan Diego in December 1531, and still
visited by thousands of pilgrims or sightseers.
Mexico dates either from the year 1325 or 1327, when the Aztecs
after long wanderings over the plateau were directed by the oracle
to settle at this spot. For here had been witnessed the auspicious
omen of an eagle perched on a nopal (cactus) and devouring a snake.
Hence the original name of the city, Tenochtitlan (nopal on a
stone), changed afterwards to Mexico in honour of the war god
Mexitli. With the progress of Aztec culture the place rapidly im-
proved, and about 1450 the old mud and rush houses wei» ruiduced*
by solid stone structures erected partly on piles amid the islets ot
Lake Tezcnco, and grouped round the central enclosure of the great
teocallL The city had reached its highest splendour on the arrival
of the Spaniards in 1519, when it comprised from 50,000 to 60,000
houses, with perhaps 500,000 inhabitants, and seemed to Cortes
"like a thing of fairy creation rather than the work of mortal
hands" (Prescott). It was at that time about 12 miles iu ciicuu*
222
M E Y =- M E Y
Ufinci~tvory where intersected by canals, anfl connectedwitUthe Tmilea from the city,/ During the Sjianish rule the cbieT' event w«fl
mainl.TBd 1))* six lon^' and solidly constructed causeways, as is clearly \ the revolt of 1692,^ when the municipal buildings wwe destroyed^
fihown by the plan fjiven in the edition of Cortcs's letters published I Since then Mexico has been tlie scene of many revolutions, and
kt Nuremberg in 1524 (reproduced in vol. iv. of H. H. Bancroft's I after the battle of Chapultepec (September 13, 1847) the city nas
Historij of the Pacific Stales, San Francisco, K.33, p. 280). After | held by the United States troops till the treaty of Guadalujit;,
its almost total destruction in November 1521, Coites employed
some 400,000 natives in rebuilding it on the same site ; but since
then the lake seems to have considerably subsided, for although
Btill .50 square miles in extent it is very shallow, and h.is retired 21
May 1848. But since the disorders ending with tho death'
Maximilian it has turned to peaceful ways, and has become a grcnt
centre of civilizing influences for the surrounding semi-barbarou*
peoples. (A. H..K.i
,'MEYEREEEE,""GlACOMO (1791-r8C.3)7first known in
Germany as Jakob Meyer Beer, was born at Berlin on
September 5, 1791,' of a wealthy and talented Jewish
family. ,■ His father, Herz Beer, was a banker ; his mother,
L^malie (nee Wulf), was a woman of liigh intellectual
•culture ; and two of his brothers distinguished themselves
in astronomy and literature. He studied the pianoforte,
first under Lauska, and afterwards under Lauska's master,
Clcmenti. When seven years old he played Mozart's Con-
certo in D Minor in public, and at nine he was pronounced
the best pianist in Berlin. For composition he was placed
under Zelter, whose lessons were soon exchanged for those
of Bernard Weber, then director of the Berlin opera, by
whom he was introduced to the Abb^ A''ogler. Struck by
his brilliant talent, Vogler invited him to Darmstadt, and
in 1810 received him into his house, wherehe formed an
intimate friend.ship with Karl JIaria von Weber, who,
though his senior by eight year.s, shared the daily lessons
he received from the abb^ in counterpoint, fugue, and
extempore organ-playing. At the end of two years the
grand-duke appointed Meyerbeer composer to the court.
His early works, how-ever, were far from successful, — his
first opera, Jephtha's Geliihde, failing lamentably at
Darmstadt in 1811, and his second, Wiiih mid Gast
(Alimelek), at Vienna in 1814. The.se checks discouraged
liim so cruelly that he feared he had mistaken his vocation.
Nevertheless, by advice of Salieri, he determined to study
vocali.'iation in Italy, and then to form a new style. But
at Venice he was so captivated by the style of Rossini that,
renouncing all thought of originality, he produced a suc-
cession of seven Italian operas — Romilda e Cnstanza,
Semiramide riconosciuta, Edouardo e Cnstina, Emma di
Hosbmyo, Marglierita d'AnJou, L'Eside di Granata, and II
Crociato in Epitto — which all achieved a success as brilliant
as it was unexpected. Against this act of treason to Ger-
man art Weber protested most earnestly ; and before long
^Meyerbeer himself grew tired of his defection, though the
success of 11 Crociato was so great that he was crowned
upon the stage. An invitation to Paris in 1S2C led him
to review his position fairly and dispassionately, and he
could not conceal from himself the fact that he was wast-
ing in imitation powers which, rightly used, might make
his name immortal. For several years after this he pro-
duced nothing in public ; but, in concert with Scribe, ho
planned the work which first made known the reality of his
transcendent genius — his first French opera, Robert le
Dinble.\ This gorgeous drama was [iroduced at the Grand
Op^ra in 1831, and received with acclamation. It was the
first of its race, a grand romantic opera, abounding ^vith
scenes of startling interest, with situations more powerfully
dramatic than any that^ had been attempted either
by Cherubini or Rossini, with mysterious horrors and
chivalric pomp, and with ballet music such as had never
yet been heard, even in Paris. ■ Its popularity exceeded all
previous expectation ; yet for five years after this signal)
triumph Meyerbeer appeared before the public no more.*.
We'c.ahnot doubt that his 'motive for^thi:? retircmentiwai!"'
thc'^etermination to produce something greater still ;-and'
"iOr. accordlD!! to some'aeco' nts;, !1'79X!
in some respects his next opera, Les Ihiguenots,' TcS\ly\KX.
greater, though it fell short of the deep romance which ren-
dered Robert le Viable so incomparably captivating.
The first performance of Les Hnr/iunots took place in
183G. In gorgeous colouring, in depth of passion, in con^
sistency of dramatic treatment, and in careful delineation
of individual character, it is at least the equal of Robert le
DiaUe. In two points only did its interest fall short of
that inspired by the earlier work. Meyerbeer had shown
himself so great a master in his treatment of the superr
natural that one regretted the unavoidable omission of
that powerful element in his second grand opera ; and,
more important still, the fifth act of Les Huguenots was so
arranged by the librettist as to render effective musical
treatment impossible. The substitution of a noisy fusiHade
I for a legitimate dramatic situation w'as fatal to the antici-
pated climax. The music which accompanies this division
of the work is necessarily inferior to all that precedes it.
The true interest of' the drama culminates at the close of
the fourth act, when Raoul, leaping from the window,
leaves Valentine fainting upon the ground. The spectator
needs not to be told that the former will be shot down the
moment he arrives in the street, or that the latter ^vill
mourn for him to the end of her days. Neither masically
nor dramatically does anything more remain to be said ;
and therefore it is that those who quit the theatre when
the curtain falls for the fourth time carry away with them
I a far more perfect ideal than those who remain to the' end.
After the production of Les JIvguenots Jleyerbeer again
I retired from public view, and spent many years in the pre-
I paration of two of his greatest works — the greatest of all
except the two we have already mentioned^ii'yi_/Vicam<
I and Le Prophcte. The libretti of both these operas were
furnished by Scribe ; and both were subjected to countless
changes of detail before they satisfied the composer's
fastidious taste ; in fact, the story of L'Africaine '..waa'
more than once entirely rewritten.
j Meanwhile Meyerbeer accepted the appointmcntjof
I kapellmeister to the king of Prussia, and spent /some
years at Berlin, where he produced Ein FeldlagerXin
Sc/desien, a German opera, in which the aiatcJilessi
I cantatrice Jenny Lind made her first' appearance 'in
' Prussia, with unprecedented success. Hero also. he com-
posed, in 1846, the overture to his brother Michael's drama,
Stntensce. But his chief care at this period was bestowed
j upon the worthy presentation of the works of others. 'He
' began by producing his dead friend Wehefs'^Eurt/ant/ie,
j with scrupulous attention to the composer's original _idea.
With equal unselfishness he procured the acceptance ^ of
I Rien::i and Der Ftiegende Ilolldndfr, the first two '.operas
I of Richard Wagner, who, then languishing in povcrty^nd
exile, would, but for him, have found it impossible _tc
obtain a hearing in Berlin. With Jenny Lind, as prima
donna and Jleyerbcer as conductor, the opera^,flourishcd
brilliantly, in, the Prussian capital; but , the'^ansicticSj^o'
this thankless period . materially^ shortened ithelcompoier's
life.' ^ . _ _ __ _.'^ ^ . _
'Meyerbeer" produced ^£(! !7'ro/)//<;^f''atTPafis' in ]819";
and, if it did not at firc.t create so great a sensation as Les
jfft/^r.'cr.o.'.'i^his was simply because it needed to Ic.bet'ei
M E Z — M I A
223
known. In 1854 he brought out L'^toile du Nord at the
Opira Comique, and in 1859 Le Pardon de Ploermel
(Dinorah). His last great work, L' Afrkaine, was in active
preparation at the Acad^mie when, on the 23d of April
1863 he was seized with a sudden illness, of which he
died on the 2d of May. . L'Africaine was produced with
pious attention to the composer's minutest wishes, on
April 28, 1865, and fully justified the expectation which
had been raised by his long and painstaking consideration
of its details. 'Upon this, in conjunction with Robert le
Diahle, Les Huguenots, and Le Prophete, his fame now
almost entirely rests.
Meyerbeer's genius has been criticized with widely different re-
mits. Mendelssohn thought his style exaggerated ; Fetis thought
him one of the most original geniuses of the age ; Wagner calls
tim "a miserable music-maker," and "a Jewish banker to whom
it occurred to compose operas." But the reality of his talent
has been recognized throughout all Europe ; and, in spite of the
acknowledged crudity of his system of phrasing, and the inequality
of merit too plainly ohserrabie even in nis greatest works, his name
will live so long as intensity of passion and power of dramatic
treatment are regarded as indispensable characteristics of dramatic
music. (W. B. E.)
M^ZlfeRES, a fortress of the first class, and the capital
of the department of Ardennes, France, is 161 miles to the
north-east of Paris by railway, on a peninsula of the
Meuse, which almost entirely surrounds the town, and
separates it from its more important suburb, CharleviUe.
The fortifications, which, as well as the citadel, are the
work of Vauban, are pierced by four gates, giving aecess
to the town, the streets of which are narrow and winding.
The parish church, erected in the 16th century, contains two
inscriptions in commemoration respectively of the raising
of the siege of iKzieres in 1521 and the marriage of
Charles IX. with the daughter of the emperor Maximilian
n., which was celebrated at M(Sziferes in 1570. The north
and south portals, the glass of the windows, and the lofty
vaultings of the church are worthy of remark. The h6tel
de viDe contains several interesting pictures relating to the
history of the town. The iron industry, the only one of
any importance, is being gradually transferred to Charle-
ville. The popiilation in 1881 was 6120.
Founded in the 9th century, Mezieres was at first only a strong-
hold belonging to the bishops of Rheims, which afterwards became
the property of the counts of Rethel. The town was increased by
successive immigrations of the people of Liege, flying first from the
emperor Otho, and afterwards from Charles the Bold ; and also by
poncessions from the counts of Rethel. Its walls were built in the
13th century, and in 1521 it was successfully defended by Bayard
'against the imperialists. The anniversary of the deliverance of the
town is still observed yearly on the 27th of September. The school
of military engineering, since transfeixed successively to Metz and
Fontainebleau, was originally founded at Mezieres.
MEZO-Tl)R,' a corporate town in the Cis-Tisian county
of J4s2-Nagy-Kun-Szolnok, Hungary, situated on the right
bank of the Beretty6, and on the railway from Arad to
Szolnok, in 47° 1' N. lat., 20- 39' E. long. It has Eoman
Catholic and Calvinist churches and schools, a judicial
court for the circuit, and the usual Government offices, but
can boast of few buildings of special interest. Horses,
oxen, and sheep are reared in great numbers on the wide-
spreading communal lands, which are productive also of
cereals, and especially wheat, rape-seed, and maize. On
the 31st December 1880 the population amounted to
20,649 (10,265 males, 10,384 females), mostly Magyars
by nationality.
MEZZOFAKTI, Gixtseppe (1774-1849), cardinal, whose
colloquial linguistic acquirements have become proverbial,
was bom, September 17, 1774, at Bologna, where his
father followed the occupation of a carpenter. Educated
first at one of the "scuole pie," and afterwards at the
' Mezii is a Magyar word, signifying Field, prefixed to many agri-
csUoral localities in Hungary.
episcopal seminary of his native city, he was ordained to
the priesthood in 1797, and in the same year became pro-
fessor of Arabic In the universitj', but shortly afterwards
was deprived on account of his refusal to take the oath of
allegiance to the Government of the Cisalpine Republic.
In 1803, however, he was appointed assistant librarian of
the institute of Bologna, and soon afterwards was reinstated
as professor of Oriental languages and of Greek. The
chair was suppressed by the viceroy in 1808, but aga^n
rehabilitated on the restoration of Pius VEL in 1814, and
continued to be held by Mezzofanti until his removal from
Bologna to Rome in 1831, when he received certain ecclesi-
astical appointments and the rank of monsignore. Mean-
while his progress in the acquirement of languages had
been rapid and untiring, and in 1833 he was appointed to
succeed Mai as chief keeper of the Vatican Library. His
promotion to the cardinalate, and the duties of director of
studies in the Congregation of the Propaganda, followed in
1838. He died at Rome, during the absence of the
pontifical court at Gaeta, on March 15, 1849.
Mezzofanti's peculiar talent, comparable in many respects to that
of the numerous "calculating boys " who have been the wonder of
their contemporaries, was not combined with any exceptional
measure of intellectual power, and accordingly produced nothing
that has not perished with him. It seems to be well established,
however, that he spoke with considerable fluency, and in some cases
even with attention to dialectic peculiarities, some fifty or sixty
languages of the most widely separated families, besides having a
less perfect acquaintance with many others. See Manavit, Esquisse
historique sur Ic Cardinal Mezzofanti, Paris, 1854 ; and Russell,
Life of the Cardinal Mezzofanti, Loudon, 1857.
MEZZOTINT. See Enoeavihg.
MIAUTSE. The Miautse or Meaou-tsze of southern
China are one of the aboriginal tribes of the country.
At one time they occupied a considerable portion of the
rich and fertile lands which now form the central province
of the empire, but as the Chinese advanced southwards
they were driven, like the Ainos in Japan and the Welsh
in Britain, into the more inaccessible districts until they
were compelled to seek refuge from the invaders in the
mountain ranges, in the provinces of Yunnan, Kwei-chow,
Kwang-se, and Kwang-tung, where they are found at the
present day. This line of mountains extends for about
400 miles, and, being in many parts high, steep, and rugged,
it forms a convenient shelter for them. As early as the
reign of king Seuen (about 800 b.c.) we read of an expedi-
tion having been sent to drive them out of Hoo-nan, and
since that time they have been periodically attacked either
to punish them for misdeeds or to make them yield up
vineyards coveted by Chinese Ahabs. The last important
campaign against them was undertaken by the emperor
K'een-lung, who, having completely subjugated the Eleuths,
was desirous of bringing under his yoke these mountain
tribesmen. But the same success which had attended his
arms in the north did not follow them to the south. The
first expedition was utterly defeated, and the general in
command paid the penalty of discomfiture with his head.
The leader of a second expedition, having learned wisdom
by the fate of his predecessor, purchased the submission of
the iliautse by a large bribe. As soon as the unsuspecting
savages had been thus lulled into security a third army
was set in motion against them. This time, being unpre-
pared, they suffered a crushing defeat, and were compelled
to purchase peace by swearing allegiance to their conquerors.
But, though the Chinese thus gained sovereignty over them,
they have since deemed it wise to content themselves with
but the shadow of authority. No real jurisdiction is ever
exercised over these hardy mountaineers. They are allowed
to govern themselves on their own patriarchal system. The
old men of each tribe manage the affairs of their juniors,
and command an obedience which would be utterly refused
to the mandate of any mandarin. In figure the Miautse.
224
M I C — 'M! I C
both men and women, are shorter and darkercomplexionej
than the Chinese, their fstces also are rounder and their
features sharper. In disposition, too, they are very unlike
their civilized neighbours. They are brave, passionate,
suspicious, revengeful, and indifferent to cold and hunger ;
they ara free and easy in their manners, and are as noisily
joyous as the Chinese are grave and sedate.
They are divided into between forty and fifty clans, each of which
is distinguished by a name which is generally derived either from
some physical characteristic, or from some custom, or from the
habitat of the clan, as, for example, "The Black Miau," "the
uarrow-headed Miau," so named from their manner of dressing
their hair, "the six-valley Miau," ic. Among these clans there
exist wide differences of culture, some being in no way removed
from savages, whileothers who have been brought under the influence
of Chinese civilization show themselves apt and ready learners.
Very few of them, so far as is known, possess any written records.
The Yaou'jin, or Goblin clan, are said to have books, which, though
th»jy are now unable to read, they still regard with reverent awe.
"The barbarous characters" used in these books are, according to a
Oiiinese writer, "like knotted worms, and are utterly unintelligible."
The Ko-los also are said to be a lettered clan, but for the most part
the Miautse content themselves with conveying information and
preserving records by means of notched sticks. Their language as
well as their ethnic characteristics prove them to be closely related to
the Siamese, Anamese, Cambodians, and the inhabitants of Hainan ;
in fact fhey form part of the race which is spread over the whole of
south-e'astem Indo-China. Their social customs are as widely
different as their appearance ia^ from those of the Chinese. The
widest latitude is given to the youth of both sexes in the choice of
their husbands and wives. As among the hill tribes of Chittagong,
the selection is commonly made on the mountain side, where on moon-
light nights in the " leaping month " the young men and maidens
meet to sing or to play at ball, or to dance round the "devil's staff"
[Anglice, Maypole), and tochoosetheirparfnersforlife. Amongsome
clans the "couvade" is an established custom. Their fuueral rites
vary according to the districts, those living within reach of the influ-
ence of the Chinese having adopted their customs, while those more
remote still hang their^ead in baskets from trees, or lay them in the
ground and disinter them yearly to wash their bones. In dress they
are fond of bright colours, and commonly wear loose but short
jackets, sometimes with and sometimes without trousers. The men
wear turbans wound rounri their hair, which is raised above the
head in the shape of a spiral shell, and the women either don a
kind of cap, or dress theu" hair in the shape of a ram's horn. For
many years the relations of the Miautse with the Chinese Govern-
ment have been generally of a peaceable nature, and in the Pck'ing
Gazette of April 1881 there was published a new system of
government by which it is hoped that the incorporation of the
mountaineers into the empire may, become more real and complete.
See Sketches of the Miaa-ULe, translated by E.G. Brldgman ; J. Edkias. The Miau-
tti Tribes, their Bistort/', and *'Quaint customs In Kwel-chow," Cornhill Magazine,
January 1872,
MICAH (^?'P) ia the short form of a name which in
various modifications — Mlco.idhu, MicdiShu, Mlcdiah — is
common in the Old Testament, expressing as it does a
fundamental point of Hebrew faith : \VTio is like Jehovah ?
The name "was borne among others by the Danite whose
history is given in Judg. xvii. sq., by the prophet who
opposed Ahab's expedition to Ramoth-Qilead (1 Kings
xxii.), and by the subject of the present article, the con-
temporary and fellow-worker of Isaiah, whose name is
prefixed to the sixth in order of the books of the minor
prophets.''
It is at- once apparent that the book of Micah divides
itself into at Least two distinct discourses, chap. \\. 1
forming a new commencement ; and from what we know
in general of the compilation of the prophetic collection we
cannot at once determine whether the second discourse,
which has no title, is to bo ascribed to iho author of the
immediately preceding prophecy, or is to be regarded as an
independent and anonymous piece. To decide this question,
if it can be decided, we must begin by a separate study of
the earlier chapters to which the title in Micah i. 1 directly
belongs. These again fall into two parts. Chaps, i.-iii.
(with the exception of two verses, ii. 12, 13) are a predic-
* A confusion between the two prophets of the name has led to the
Inaertion in the Masaoretic text of 1 Kir.fjs Xiii. 28 of a citation from
Micah i. 2, rightly absent from the LiX.
tion of judgment on the sins of Judah and Ephraim. Ia
a majestic exordium Jehovah Himself ia represented aa
coming forth in the thunderstorm (comp. Amos L 2) from
His heavenly palace, and descending on the mountains of
Palestine, at once as witness against His people, and the
eiecuter of judgment on their sins. Samaria is sentenced
to destruction for idolatry ; and the blow extends to Judah
also, which participates in the same guilt (chap. i.). But,
while Samaria is summarily dismissed, *he sin of Judah is
analysed at length in chaps, n. and iii., in which the prophet
no longer deals with idolatry, but with the corruption of
society, and particularly of its leaders — the grasping
aristocracy whose whole energies are concentrated on
devouring the poor and depriving them of their little
holdings, the unjust judges and priests who for gain
wrest the law in favour of the rich, the hireling and
gluttonous prophets who make war against every one
"that putteth not into their mouth," but are ever ready
with assurances of Jehovah's favour to their patrons, the
wealthy and noble sinners that fatten on the flesh of the
poor. The prophet speaks with the strongest personal
sympathy of the sufferings of the peasantry at the hands
of their lords, and contemplates with stem satisfaction the
approach of the destroyer who shall carry into e.xile " the
luxurious sons" of this race of petty tyrants (i. "16), and
leave them none to stretch the measuring line on a field in
the congregation of Jehovah (ii. 5). The centre of corrup-
tion ia the capital, the city of Zion, grown great on the
blood and wrongs of the provincials, the seat of the cruel
princes, the corrupt judges and diviners. For their sake,
he concludes, Zion shall be plowed as a field, Jerusalem
shall lie in ruins, and the temple hUl return, to jungle
(iii. 12).
The situation thus sketched receives its elucidation from
the data supplied by the title (i. 1) and confirmed ant',
rendered more precise by a remarkable passage in Jeremic.li.
According to the title Micah flourished in the reign.'; of
Jotham, Ahaz, and Hezekiah ; according to Jeremiah
(xxvi. 18 sq.) the prophecj-of the destruction of Jerusalem
just cited was spoken under Hezekiah, and bore fruit in
the repentance of king and people, by which the judgment
was averted. The allusion beyond doubt is to Hezekiah's
work of religious reformation (2 Kings xviii. 4 sq.). It is
hardly possible to separate this reformation from the influ-
ence of Isaiah, which did not become practical in the
conduct of the state till the crisis of Sennacherib's invasion ;
and the conclusion that Hezekiah was not from the first a
reforming king, which is forced on us by many passages of
Isaiah, is confirmed by the prophecy of Micah, which, after
Hezekiah's accession, still represents wickedness as seated
in the high places of the kingdom. The internal disorders
of the realm depicted by Micah are also prominent in
Isaiah's prophecies ; they were closely connected, not' only
with the foreign complications due to the approach of the
Assyrians, but with the break-up of the old agrarian
system within Israel, and with the rapid and uncompen-
sated aggrandisement of the nobles during those pro-
sperous years when the conquest of Edom by Amaziah
and the occupation of the port of Elath by his son
(2 Kings xiv. 7, 22) placed the lucrative trade between
the Mediterranean and the Rod Sea in the hands of
the rulers of Judah. On the other hand the democratic
tone which distinguishes Micah from Isaiah, and his
announcement of the impending fall of the capital (th»
deliverance of which from the Assyrian appears to Isaiah
as the ni^cessarj- condition for the preserv'ation of the seed of
a new a^J better kingdom), are explained by the fact that,
while Isaiah lived in the centre of affairs, Micah was a
Moraathi;-' or inhabitant of Moresheth Oath, a place near
the Philistine frontier so unimportant as to be mentioned
M I C A H
225
only in Jlicah L i4.* The provincial prophet sees the I
capital and the aristocracy entirely from the side of a man.
of the oppressed people, and foretells the utter ruin of both.
But this ruin does not present itself to him as involving
the captivity or ruin of the nation as a whole ; the
congregation of Jehovah remains in Judsea when the
oppressors are cast out (ii. 5) ; Jehovah's words are still
good to them that walk uprightly ; the glory of Israel is
driven to take refuge in Adullam, as in the days when
David's band of broken men was the true hope of the
nation, but there is no hint that it is banished from the
land. Thus upon the prophecy of judgment we naturally
eipect to follow a prophecy of the redintegration of
Jehovah's kingship in a better Israel, and this we find in
ii. 12, 13 and in chaps, iv., v. Both passages, however,
present diflSculties. The former seems to break the pointed
contrast between Ii: 11 and iii. 1, and is therefore regarded
by Ewald as an example of the false prophecies on which
the wicked rulers trusted. The thought, however, is one
proper to all true prophecy (comp. Hos. i. 11 [ii. 2], Isa.
si. 11 sq., Zeph. iii. 14, Jer. xxxi. 8), and precisely in
accordan-i with chaps, iv., v., even in the details of expres-
sion and imagery.* It is indeed possible that these verses
are a separate oracle of Micah, which did not originally
stand in its present connexion. The sequence of thought
in chaps iv., v., on the other hand, is really difiicult, and
lias given rise, to much complicated discu-ssion.^ There is a
growing feeling among scholars that iv. 11-13 stands in
direct contradiction to iv. 9, 10, and indeed to iii. 12.
The last two passages agree in speaking of the capture of
Jerusalem, the first declares Zion inviolable, and its capture
an impossible profanation. Such a thought can hardly be
Micah's, even rf we resort to the violent harmonistic process
of imagining that two quite distinct sieges, separated by a
lenewal of the theocracy, are spoken of in consecutive
verses. An interpolation, however, in the spirit of such
passages as Ezek. xxxviii., xxxix.j Joel iii. [iv.], Zech. siv.,
•3 very conceivable in post-exilic times, and in connexion
.vith the growing impulse to seek a literal harmony of all
prophecy on lines very different from the pre-exilic view
in Jer. xxvi., that predictions of evil may be averted by
repentance. Another difficulty lies in the words "and
thou shalt come even to Babylon" in iv. 10. Micah
'jnquestionably looked for the destruction of Jerusalem as
' Tliat Micah lived in the Shephela or Judx;\n lowland near the
Philistine country is dear from the local colouring of i. 10 sg., where
n number of places in this quarter are mentioned together, and their
names played upon in a way that could hardly have suggested itself
to any but a man of the district. The paronomasia makes the verses
difficult, and in i. 14 nono of the ancieut versions recognizes More-
sheth Gath as a proper name. The word Morasthite {Mdrtishti) was
therefore obscure to thera ; but this only gives greater weight to the
traditional pronunciation with d in the first syllable, which is as old
as the I.XX., and goes against the view, taken by the Targum both on
Micali and on Jeremiah, and followed by some modems (including
Roorda), that Micah came from Mareshah. When Eusebius places
MupatrOfi near £l6uthert)poli3 it is not likely that ho is thinking of
Mareshah (Mai-esa), for he speaks of the former as a village and of the
latter as a ruin 2 miles from Eleutheropolis. Jerome too in the
Epic. PaxUa {Ep. cvui.), speaking as an eye. witness, distinguishes
Morasthim, with the church of Micah's sepulchre, from Maresa. This
indeed was after the.pretended miraculous discovery of the relics of
Micah in 385 A.D. ; but the name of the village which then existed
{Prmf. in Mich.) can hardly have been part of a pious fraud. . '*■ •
' The figure of the shepherd gathering a scattered flock certainly
does not presuppose a total captivity, as Stade {Z. /. AT. IF., i. 161
«7.) argues. . v-»- ■,.
.•See.besidesthecommentaries, Noldekeinthe SiW-Jer.; iv. 21i; a
paper by Oort and two by Kuenen in Theol. TijdKh., 1872; Well-
■hausen-Bleek, Einkitung, p. 426; Stade, I.e., and ibid., iii. 1 57.
Stade goes so far as to malte the whole of Micah iv., v. presuppose the
exile, and to find still latef additions in iv. 5-10., v. 5, 6 [v. 4, 6].
Jfcsebrecht, Tkcol. LZ., 1381, col. 443 sj., rejects chap. iv. only.
^0 arguments cannot be here cited at length, but they are tacitly
upt in view in what follows
well as of Samaria in the near future and by the Assyrians
(i. 9), and this was the judgment which Hezekiah's repent-
ance averted. If these words, therefore, belong to the
original context, they mark it as not from Micah's hand ;
but it is easy to see that they are really a later gloss. The
prophetic thought is that the daughter (population) of Zioii
shall not be saved by her present rulers or defensive
strength; she must come down from her bulwarks and
dwell in the open field ; there, and not within her proud
ramparts, Jehovah will grant deliverance from her enemies.
This thought is in precise harmony with chaps, i.-iii., and
equally characteristic is what follows in chap. v. Slicah's
opposition to present tyranny expresses itself in recurrence
to the old popular ideal of the first simple Davidic kingdom
(iv. 8) to which he had already alluded in i. 15. These
old days shall return once more. Again guerilla bands
(inrna) gather to meet the foe as they did in the time
of Philistine oppression. A new David, like him whose
exploits in the district of Micah's home were still in the
mouths of the common people, goes forth from Bethlehem
to feed the flock in the strength of Jehovah. The kindred
Hebrew nations are once more united to their brethren of
Israel (comp. Amos ix. 12, Isa. xvi. 1 eq.). The remnant
of Jacob springs up in fresh \-igour, inspiring terror among
the surrounding peoples, and there is no lack of chosen
captains to lead them to victory against the Assyrian foe.
In the rejuvenescence of the nation the old stays of that
oppressive kingship which began with Solomon, the strong-
holds, the fortified cities, the chariots and horses so foreign
to the life of ancient Israel, are no more known ; they
disappear together with the divinations, the soothsayers,
the idols, the jiiag^ebas and asheras of the high places
Jehovah is king on Mount Zion, and no invention" of man
come between Him and His people.
The elements of this picture, drawn so largely from the
most cherished memories of the Judseans, could not fail to
produce a wide impression, especially when the invasion of
Sennacherib, although it spared Jerusalem, fulfilled in the
most striking ■n-ay a great part of Micah's predictions of
judgment. Of this we have evidence", not only in Jer. xxvi.,
but in the political and religious ideas of the book of
Deuteronomy. The picture of the right king (Deut. xvii.
14 sj.) and the condemnation of the high-places alike
follow the doctrine of Micah.
A difficulty still remains in the opening verses of chap. iv.
Micah iv. 1-3 and Isa. ii. 2-4 are but slightly modified recensions
of the same text, and as Isa. ii. is older than the prophecy of Micah,
while on the other hand Micah iv. 4 seems the natural completion
pf the passage, it is common to suppose that both copy an older
prophet. But the words have little connexion with the context in
Isaiah, and may be the quotation of a copyist suggested by ver. 5.
On the other hand it has been urged that the pa.ssage belongs to a
later stage of prophetic thought than the 8th century B.C. There
is, however, no real difficulty in the idea that foreign nations shall
seek law and arbitrament at the throne of the king of Zion (comp.
the old prophecy Isa. xvi.); and the mention of the temple as the
seat of Jeliovah's sovereignty may he illustrated by Isa. vi., where the
heavenly palace (Micah i. 3) is at least pictured in the likeness of the
temple on Zion. At the same time the Jerusalem of Micah iv. 8
is the Jerusalem of David not of Solomon, the ideas of iv. 1-4 do
not reappear in chap. v. , and the whole prophecy would perhaps be
more consecutive and homogeneous if iv. 6 (where the dispersed and
the suffering are, according to chap. ii. , the victims of domestic not
of foreign oppression) followed directly on iii. 12.
The sixth chapter of Micah presents a very different situation
from chaps, i.-v. Jehovah appears to plead with his people for their
sins, but the sinners are no longer a careless and oppressive aristo-
cracy buoyed up by deceptive assurances of Jehovah's help; by pro-
phecies of wine and strong drink ; they are bowed down by a
religion of terror, wearied with attempts to propitiate an ongry God
by countless offerings, and even by the sacrifice of the first-bom.
Meantime the sub.stance of true religion — justice, charity, and a
humble walk with God— is forgotten, fraud and deceit reign in all
classes, the works of the house of Ahab are observed (worship of
foreign gods). Jehovah's judgments are multiplied against the
laud, and the issue can bo nothing else than its total desolation. All
XVI. — 20
226
MIC — M 1 C
tnese marks fit exactly the evil times of jranasseh as described in
2 Kings xxi. Chap. vii. 1-6, in whirli the public and private cor-
ruption of a hopijess ago is bitterly bewailed, obviously belongs to
the same context (comp. vol. xiii. p. 415).. Jlicah may very well
have lived into Manasseh's reign, but the title in i. 1 does not cover
a pronhecy which certainly falls after Hezekiah's death, and the
style has nothing in common with tlie earlier part of tlie book. It
is tlierefore prudent to regard the pronhecy, with Ewald, as anony-
mous. Ewald ascribes the whole of chaps, vi., vii. to one author.
Welihausen, however, remarks with justice that the thread is
abruptly broken at vii. 6, and that verses 7-20 represent Zion as
already fallen before the heathen and her inhabitants as pining in
the darkness of captivity. The hope of Zion is in future restora-
tion after she has patiently borne the chastisement of her sins.
Then Jehovah shall arise mindful of His oath to the fathers, Israel
sliall be forgiven and restored, and the heathen' humbled. Tlie faith
and hope whi^h breathe in this passage have the closest affinities
wich the book of Lamentations and Isa. xl.-!xvi.
Wc have seen that the text of MIcah has suffered from redactors ; it Is also not
free from verb.il corruptions \vhlch make sc.mo places very obscure. The LXX
had many readmga dlHerent from the present Hebrew, but tb'eir text too was far
fiom sound. Of commentaries on Micah, that which deals most fully with the
question of the text Is Roorda's Latin work, Lcyden, 186!). The most elaborate
book on .Mleah Is Casparl's (Utrber ilicha den iloratthilen uud seine prophet isdie
Srhh/l, Chrlstiania, 1851-02). In EnRllsh Pocock's Commentary <2d cd., 1CD2)
and Cheytie's ificah (1832) arc to be noted. See also the literature on the minor
Fi'o°i''r" '" ecncral cited under Hosea, and W. R. Smith's Prophets of Isra
C™^)' , (W. R. S.)
MICHAEL (?!<3'P, " who is like God ! ") appears in the
Old Testament as a man's name, synonj-mous with Mieaiah
or Micah. In the book of Daniel the same name is given
to one of the chief " princes " of the heavenly host, the
guardian angel or " prince " of Israel (Dan. x. 13, 21 ; xii.
1), and as such he naturally appears in Je\vish theosophy
as the greatest of all angels, the first of the four who
surround the throne of God (see Gabriel). It is as
guardian angel of Israel, or of the church, the true Israel,
that Michael appears in Jude 9 and Kev. xii. 7. In the
Western Church the festival of St Michael and All Angels
(Michaelmas) is celebrated on September 29th ; it appears
to have grown out of a local celebration of the dedication
of a church of St Michael either at Mount Garganus in
Apulia or at Rome, and was a great day by the beginning
of the 9th century. The Greek Church dedicates
November 8 to St Michael, St Gabriel, and All Angels.
MICHAEL, the name of several Byzantine emperors.
Michael I. (Rhangabe) was an obscure nobleman
who had married Procopia, the daughter of Nicephorus I.,
and been made master of the palace ; his elevation to the
throne was due to a revolutionary movement against his
brother-in-law Stauracius, who reigned only two months
after the death of Nicephorus on the battlefield (812).
Elected as the tool of the bigoted orthodox party in the
church, Michael diligently persecuted the Iconoclasts on
the northern and eastern frontiers of the empire, but
meanwhile allowed the Bulgarians to ravage a great part
of Macedonia and Thrace ; having at last taken the field
in the spring of 813, he was defeated near Bersinikia, and
Leo the Armenian was saluted emperor in his stead in the
following summer. Michael, after having been compelled
to become a monk, was permitted thenceforward to live
unmolested in the island of Prote, where he died in 845.
Michael II. (Tlie Stammerer), a native of Amorium
in Phrygia, was of humble origin, and began life as a
private soldier, but rose by his talents and assiduity to the
rank of general. He v.'as one of those who had favoured
the election to the throne of his old companion in arms
Leo the Armenian in 813, but, detected in a conspiracy
against the government of that emperor, had been sentenced
to death in December 820 ; his partisans, however, suc-
ceeded in assassinating Leo on the morning of Christmas
Day, and called Michael from the prison to the throne.
The principal features of his reign (820-829) were a pro-
tracted struggle (of nearly three years) against his brother
general, Thomas, who aimed at the throne, the conquest
of Crete by the Saracens in 823, and the beginning of thc'r
attacks upon Sicily (827). Conciliatory on the whole
I in his policy towards the image worshippers (Lis own
.sympathies were iconoclastic), he incurred the wrath of the
monks by entering into a second marriage with Euphrosyne,
daughter of Constantino VL, who had previously takea
the veil. He died in October 829, and was succeeded by
Theophilus his son.
Michael HI. (The Drunkard) was the grandson of
Michael the Stammerer, and succeeded his father Theophilus
when only three years of age (842). Until his majority
at tba age of eighteen the aflairs of the empire were
managed by the empress-regent his mother Theodora ; his
education was shamefully neglected, and it was during this
period that Michael formed the disgraceful personal habits
which are indicated by his surname. In 861 Michael,
together with his uncle Bardas, undertook an expedition
againsit the Bulgarians, which resulted in the con%ersion of
the Bulgarian king, who thenceforth bore the Christian
name of Michael. The emperor had been less successful
in the campaign which he led in person against Omar of
Melitene in 860, but in 863 his imcle Petronas gained an
important victory over the Saracens in Asia Jlinor. The
year 865 was marked by the first appearance of the Russians
in the Bosphorus. Michael was assassinated in his palace
in 867 by Basilius the jiacedonian, whom he had associated
with himself in the empire in the previous year.
Michael IV. (The Paj'hlagonian) owed his eleva-
tion to Zoe, daughter of Constantino IX., the last of
the Macedonian dynasty ; this princess was married to
Romanus HI., but becoming enamoured of Michael, her
chamberlain, she poisoned her husband and married her
attendant (1034). Jlichael, however, being of a weak
character and subject to epileptic fits, possessed the supreme
power only in name, and was a mere instrimient in the
hantls of his brother, John the Eunuch, who had been first
minister both of Constantine and Romanus. John's
diplomacy was successful in keeping the Arabs in the
archipelago and Egj'pt quiet for some lime, and he was
at last able to secure a victory for the imperial arms at
Edessa in 1037. The attempt to recover Sicily in the
following year with the help of the Normans was less pro-
sperous, and in 1040 the island wholly ceased to be a
Byzantine province. About the same time, the Bulgarians
having overrun Macedonia and Thrace, and threatening
Constantinople, the indolent and infirm emperor, to the
surprise alike of friends and foes, put himself at the head
of the army, and not only drove the enemy beyond the
frontier, but followed them into their own territory. He
died, shortly after his triumph, on December 10, 104L
Michael V. (Calaphates or The Caulker), nephew
and successor of the preceding, derived his surname from
his father Stephen, who had originally followed the occu-
pation of a caulker of ships. He owed his elevation
(December 1041) to his uncle John, whom -along with Zoe
he almost immediately banished ; this led to a popular
tiunult and his dethronement after a brief reign of four
months (April 1042). He lived for many years afterwards
in the quiet obscurity of a monastery.
JticHAEL VI. (The Warlike) was already an old man
when chosen by the empress Theodora as her successor
shortly before her death in 1056. His government was
feeble in the extreme, and he was at last compelled to
abdicate by Isaac Comnenus, who had defeated his army in
Phrygia (August 1057). He also spent the rest of his life
in a monastery.
Michael VII. (Ducas or Parapinaces) was the eldest
son of Constantine XL Ducas, by whom along with his
brothers Andronicus I. and Constantine XII. he was
invested with the title of Augustus ; this joint succession
took place in 1067, but in 1071 it suited the policy of the
uncle Joannes Ca-sar to make Michael sole emperor. For
M I C — M I C
227
Ihis 'position Michael, whose " character was degraded,
rather than ennobled, by the virtues of a monk and the
learning of a sophist," was by no means fitted, and at
length two generals of the name of Nicephorus, surnamed
Bryennius and Botaniates, simultaneously rebelled against
him in 1078 ; with hardly a struggle he resigned the purple
and retired into a monastery, where he afterwards received
the title of archbishop of Ephesus.
Michael VIII. (Palaeologus), born in 1234, was the
son of Andronicus Palaeologus Comnenus and Irene
Angela the granddaughter of Alexius Angelas, emperor
of Constantinople. At an early age he rose to distinc-
tion, and ultimately became commander of the French
mercenaries in the employment of the emperors of
Nicsea. A few days after the death of Theodore Lascaris
n. in 1259, Michael, by the assassination of Muzalon
(which he is believed but not proved to have encouraged),
sncceeded to the guardianship, shared with the patriarch
Arsenius, of the young emperor John Lascaris, then a lad
of only eight years. Afterwards invested with the title of
"despot," he was finally proclaimed joint-emperor, and
crowned alone at Nicsea on January 1, 1260. In the
following year (July 1261) Constantinople fell into the
hands of the Caesar Alexius Strategopulus, and Michael,
having got himself crowned anew in the church of St
Sophia, caused his boy colleague to be blinded and sent
into banishment. For this last act he was excommunicated
by Arsenius, and the ban was not removed until six years
afterwards (1 268), on the accession of a new patriarch. In
|l263 and 1264 respectively Michael, with the help of
[Urban IV., concluded peace with Villehardouin, prince of
'Achaia, and Michael, despot of Epirus, who had previously
been incited by the pope to attack him ; the friendly inter-
vention had been secured by a promise on the emperor's
part to help forward the reunion of the Eastern and
rtVestern churches. In 1269 Charles of Sicily, aided by
Uohn of Thessaly, again made war with the alleged purpose
of restoring Baldwin to the throne of Constantinople, and
pressed Michael so hard that ultimately, yielding to the
importunities of Gregory X., he caused the deputies of the
OEastern church to attend the council of Lyons (1274) and
there accept the "filioque" and papal si^iremacy. The
iiinion thus brought about between the two churches was,
however, extremely distasteful to the Greeks, and the
persecution of his " schismatic " subjects to which , the
emperor was compelled to resort weakened his power so
much that Martin IV. was tempted to enter into alliance
with Charles of Anjou and the Venetians for the purpose
of reconquering Constantinople. The invasion, however,
failed, and Michael so far had his revenge in the " Sicilian
Vespers," which he helped to bring about. He died in
Thrace in December 1282, and was succeeded by his son
Andronicus II.
Michael IX. (PalKologus) was the son of Andronicus
n., and was associated with him on the throne from 1295,
but predeceased him (1320).
MICHAELIS, JoHAisw David (1717-1791), one of
Ine most influential scholars and teachers of last century,
belonged to a family which had the chief part in main-
taining that solid discipline in Hebrew and the cognate
languages which distinguished the university of Halle in
the period of Pietism. Johann Heinrich Michaelis (1668-
1738) was the chief director of Francke's Collegium
Orientate Theologicum, a practical school of Biblical and
Oriental philology then quite unique, and the author of an
annotated Hetrew Bible and various exegetical works of
reputation, esnecially the Adnotationes uberiores in Hagio-
graphos, 1720. In his chief publications J. H. Michaelis
Aad as fellow-worker his sister's son Christian Benedict
Michaelis (1680-1764), the father of Johann David, who
was likewise influential as professor at Halle, and a very
sound scholar, especially in Syrlao. J. D. Michaelis was
trained for academical life under his father's eye. Halle
was not then the best of universities ; a narrow theological
spirit cramped all intellectual activity, and the eager viva-
cious youth, already distingiiished by a love for realities and
a distaste for small pedantries, found much of the teaching
wearisome enough. He acquired, however, a good know-
ledge of the Latin classics, — Greek, he tells us, was hardly
taught at all, and his knowledge of Greek literature was
gained by his own reading in later years, — learned all that
his father could teach, and was influenced, especially in
philosophy, by Baumgarten, the link between the old
Pietism and Semler, while he cultivated his strong taste for
history under Ludwig. In the winter-semester 1739-40
he qualified as university lecturer. One of his disserta-
tions was a defence of the antiquity and divine authority
of the vowel points in Hebrew. His scholarship still
moved in the old traditional lines in which no further pro-
gress was possible, and he was also much exercised by
religious scruples, the conflict of an independent mind with
that submission to authority at the expense of reason
encouraged by the type of Lutheranism in which he had
been trained. A long visit to England in 1741-42 lifted
him out of the narrow groove of his earlier education. In
passing through Holland he made the acquaintance of the
great. Schultens, w-hose influence on his philological views
was not immediate, but became all-powerful a few years
later. England offered to him no such commanding per-
sonal influence, and he was not yet able to turn to profit
the stores of the great libraries, but his personality was
strengthened by contact with a larger life, and his theo-
logical views were turned aside from the pietistic channel.
Michaelis never ceased to regard himself as essentially
orthodox, though he did not feel able fuUy to subscribe
the Lutheran articles, and more than once declined on this
account to be professor of theology. But his views
acquired a distinctly rationalistic complexion, and the
orthodoxy of his Gottingen lectures and publications on
dogmatic (delivered from a philosophical chair) is of a very
washed-out kind. His really useful work, however, lay in
other directions ; the change of his theological views was
important because it relieved him from trammels that
hampered the free course of his development as a scholar.
From England Michaelis went back to Halle ; but he felt
himself out of place, and in 1745 gladly accepted an
invitation to Gottingen as privat-docent. In 1746 he
became extraordinary, in 1750 ordinary, professor, and in
Gottingen he remained till his death in 1791. In the first
years of his new position Michaelis passed through a second
education. In the young and intellectually ligorous
Georgia Augusta he came under the powerful personal
influence of such men as Gesner and Haller. His intellect
was active in many directions ; universal learning indeed
was perhaps one of his foibles. Literature — modern as
well as ancient — occupied his attention ; one of his works
was a translation of four parts of Clarissa ; and translar
tions of some of the then current English paraphrases on
BibUcal books manifested his sympathy with a school
which, if not very learned, attracted him by its freer air.
His Oriental studies were reshaped by diligent perusal of
the works of Schultens ; for the Halle school, with all its
learning, had no conception of the principles on which a
fruitful connexion between Biblical and Oriental learning
can be established. His linguistic work indeed was always
hampered by the lack of MS. material which is felt in his
philological writings, e.g., in his valuable Supplementa to
the Hebrew lexicons (1784-92).' He could not become
1 By a strange fortune of war it was the occupation of Gottingen ty
tUe FreQcli in the Seven Years' Wai-, and tie friendly relations he
228,
JM I c — n I 0
such an Arabist as Keiske ,• an J, thcugli for many years the
■most famous teacher of Semitic languages in Europe, he
had little of the higher philological faculty, and neither his
grammatical nor his critical work, highly praised as it then
was, has left a permanent mark, with the exception perhaps
of his text-critical studies on the Peshito.^ His tastes were
all for realia — history, antiquities, especially geography
and natural science ; in his autobiography he half regrets
that he did not choose the medical profession. Here he
found a field h;ydly touched since Bochart, in whose foot-
steps he followed in the Spicilegium geor/raphis Hehfsoyum
f.iierse post Bochartitm (1769-80). To his impulse we owe
the famous Eastern expedition of Von Haven, Forskal, and
Niebuhr. He prepared the instructions for their journey,
and drew up a series of questions and elucidations to guide
their researches, which place in strong relief his com|ire-
hensive grasp of all that was then known of the East, and
the keen delight in the knowledge of tangible and natural
things, paired with a sober and patient judgment, which
was his chief intellectual characteristic. The best part of
this knowledge was turned to the profit of Biblical study ;
in his exegetical writings, for exami)le, one of the main
features is what was then the novelty of illustrations from
Eastern travel. In sjiite of his doctrinal writings — which
at the time made no little noise, so that his Compenduun
of Dogmatic (1760) was confiscated in Sweden, and the
knighthood of the North Star was afterwards given him in
reparation — it was the natural side of the Bible that really
attracted him,' and no man did more to introduce the
modern method of studying Hebrew antiquity as an
integral part of ancient Eastern life. The permanent
influence of his works indeed has not been great, and many
of them are now hartUy readable ; for, with all his historic
tastes and learning, he had no large historic conceptions,
and, what is. closely akin to this defect, was singularly
deficient in imagination and poetic sympathy. But the
"vivacity of his mind, his manysidedness, his singularly
attractive though discursive method of lecturing, and
abpve all his power of feeling and inspiring interest in
every kind of fact, was a potent stimulus much needed in
the Germany of that age, and did not soon die. Different
as the three men are, there is a true historic nexus between
the three great Gottingeu Orientalists, ilichaelis, Eichhorn,
and Ewald.
The personal char.icter of Jlichnelis can be read between the lines
of his autobios^i-nphy with the aid of tlie otlier ni.it.-rials collected
by the editor Hassencarap (/. D. Michnchs LcbciisbL-scfin-ibiDirj, kc,
1793). ■ To imderstaiKl the secret of his enonnous iiillueiice, it is
not enoii|;h to read liis books, now for the most part dull cnoiij^'h
to us ; we must see the U|iri^Kt vivacious laborious nian, with a
good deal of worhlly prudence and a f;ood deal of temper, much
absorbed in his manifold academic activities in the university and
Koyal Society of Goltingen, yet ever full of interest in the larger
world, and of shrewd judgments and lively talk, with a stroiif: sense
of his rights and dignity, yet with a good and warm heart ; sjiining
especially in the lecture-room, where he dealt forth knowledge with
discursive hand from a fall .store, displaying the mctlioils as well as
the results of his all-sided research, not witliout a touch of the vanity
of the polyhistor, and loviiig to leave the chair under a storm of
applause at a parting bon-mot which he acknowledged at the door
in a backward glance of triumph. The same volume contains a
full list of his works. Besides those already mentioned it is suffi-
cient to refer to his New Testament Intmludion (the first edition,
1750, preceded the lull development of his powers, and is a very,
different book from the later editions), his rc)>rint of Lowth's
Prxlcdiones with important additions (1758-(i2), his Gerinau
translation of the Bible with notes (1773-92), his Oricntalischc
wul Excgdische BibUothck (1776-.8.'>), and Xcuc 0. ami E. Bib.
(1786-91), his l/oiaischcs Kecht (1770-71), and his eilition of
Castle's Lexicon Syriaaim (1787-88). His LiUerarisdur Brief-
KYcAsfi (1794-96) contains much that is interesting for the history
of learning in his time. (W. R. S.)
formed with the officers, that procured him tbe P»ria MS. from which
he edited Abulfeilii's description of Esypt.
i.CuTX in AcUs Aposlolonim Syriacos, 1755,
-MICHAUD, Joseph (1767-1839), French historian
and publicist, was born of an old family on June 19, 1767,
at 'Albens, Savoy, was educated at Bourg-en-Bresse, and
afterwards engaged in literary work at Lyons, where the
events of 17S9 first called into activity the dislike to
revolutionary principles which manifested itself throughout
the rest of his life. In 1791 he went to Paris, where, not
without danger, he took part in editing .several royalist
journals. In 1794 he started La Quotidienne, for his con-
nexion with which he was arrested after the 13th of
Vendemiaire; he succeeded in escai)ing his cajitors, but was
sentenced to death p<ir conlnmuce by the military council.
Having resumed the editorship of his newspaper on the
establishment of the Directory, he was again proscribed on
the 18th of Fructidor, but at the close of two years
returned to Paris when the consulate had superseded the
Directory. Hii Bourbon sympathies led to a brief
imprisonment in 1800, and on his release he for the time
abandoned journalism, and began to write or edit books.
Along with his brother and two colleagues he publi.-,hed in
1808 a Biographic modenie, on didi'Muaire des hommu
qm se sont fait nn nom en Europe depuis 1789, the earliest
work of its kind ; in 1808 tlie first volume of his Histotrc
des Croisades appeared, and in ISll he originated the
BiugrajJtie Cnirersel/e. In 1814 he resumed the editor-
ship of the Quotidienne, and in the same year was elected
Academician. In 1815 his brochure entitled llistoire dis
qnin:e Sdaaines ou le dernier regne de Bonaparte met
with extraordinary success, passing through twenty-seven
editions within a very .short time. His political servicss
were now rewarded with the cross of an officer in the Legion
of Honour and the modest post of king's reader, of which
last he was deprived in 1827 for having opposed Peyronnet's
" Loi d'Amour " against the freedom of the press. In
1830-31 he travelled in Syria and Egypt for the purpose
of collecting additional matepials for the llistoire des
Croisades ; his correspondence with a fellow explorer,
Poujoulat, consisting jiractically of discussions and eluci-
dations of various important points in that work, was
afterwards published (Con-espondance d'Orient, 7 vols.,
183-2-35). The Billiot/ieqve des Croisades, in four
Tohmies more, contained the "pieces justificatives " of the
J/is/oire. Michaud died on September 30, 1839, at Passy,
wlicre his home had been since 1832. His llistoire des
Croisades was published in its final form in six volumes in
1841 imder the editorship of his fr'cnd Poujoulat (9th ed.,
with appendix, by Huillard-Brvholles, 1856). Micliaud
along with Poujoulat also edited and in part wrote Xouvelie
Collection des Menioires povr servir a I'lJisloire de Franee.
32 vols., 1830-44. gee Sainte-Beuve, Ca«s<ries du
Ltiddi, vol. vii.
MICH.\UX, A.\DRE (1746-1802), a French botanist,
best known for his works on the Hora of North America
and as a botanical traveller. In 1779 he .spent some time
botanizing in England, and in 1780 he explored Auvergne,
the Pyrenees, and the north of Spain. In 1782 he was
sent by the French Government on a botanical mission to
Persia. His journey began unfavourably, as he was
robbed by .\rabs of all his equijiments except his books ;
but he gained influential support in Persia, having cured
the shah of a dangerous illness. After two years he
returned to France with a fine herbarium, and also intro-
duced numerous Eastern plants into the botanic gardens
of France. In 1785 he was sont by the French Govern-
ment to North America, and travelled through Canada,
Nova Scotia, and the Uniteil States as far west as the
Mississilipi. The outbreak of the French P>evolution
deprived him 'of means to continue his work in America,
and in 1 796 he returned to France. Ke was shipwrecked,
>and lost most of his collections on the voyage. In 1800
M I C — M I C
220
he went to Madagascar to investigate the flora of that
islapd, and died there in 1802. His work as a botanist
j^as chiefly done in the field, and he added largely to what
was previously known of the botany of the East and of
America. He also introduced many plants into Euro-
pean botanic gardens. He wrote two valuable works on
North-American plants,— the Histoir'. des chines de
I'Aniirique Septentrionah (1801), with 36 plates, and the
Flora Boreali-Americana (1803), 2 vols., with 51 plates.
MICHAU.X, Fra-v^ois Andk^ (1770-185.5), son of the
f)receding, was, like his father, employed by the French
Government to explore the forests of North America with
\ view to the introduction into France of trees valuable
or their wood or other products. He was very success-
'ul in carrying out this object. He published in 1810-13
a Histoire des Arhres forestieres de VAmeriquc Septunliionale,
in 3 vols., with 156 plates, a work full of information on
the characters, uses, distribution, and other points of
interest in the various species. In 1817-19 a translation
of it appeared under the title Korlh American Syha.
He also ^vrote a Voyage a Vmiest des Jlonls AUe^kanys,
1804, besides articles in scientific magazines.
MICHELANGELO (147.5-1564). Michelangelo Buon-
irroti, best known simply as Michelangelo, the last and most
famous of the great artists of Florence, was the son of
Ludovico Buonarroti, a poor gentleman of that city, and of
his wife Francesca di Neri. Ludovico was barely able to
live on the income of his estate, but made it his boast that
he had never stooped to add to it by mercantile or mechani-
cal pursuits. The favour of the Medici procured him em-
ployment in some minor ofiBces of state, and in the autumn
of 1474 he was appointed resident magistrate of Caprese,
in the Casentino, for a period of si.K months. Thither he
accordingly repaired with his family, and there, on March
6, 1,475, his second son Michelagniolo or Michelangelo was
born. Immediately afterwards the family returned to
J"lorencc, and the child was put to nurse with a niarble-
jworker's wife of Settignano. His nwther's^ health had
already, it would seem,' begun to fail ; at all events in
about two years from this time, after she had borne her
husband two more sons, she died. While still a young
boy, Michelangelo determined in spite of his father's
opposition to be an artist. Ho had sucked in the passion,
as he himself used to say, with his foster-mother's milk.
After a sharp struggle, his stubborn will overcame his
father's pride of gentility, and at thirteen he got himself
articled as a paid assistant in the workshop of the brothers
Ghirlandaio. Domenico Ghirlandaio, bred a jeweller, had
become by this time the foremost painter of Florence. In
his service the young Michelangelo laid the foundations
of that skill in fresco with which twenty years afterwards
he confounded his detractors at Rome. He studied also,
like all the Florentine artists of that age, in the Brancacci
chapel, where the frescos of ^^asaccio, painted some sixty
years before, still victoriously held their own; and here, in
a quarrel with an ill-conditioned fellow-student, Torrigiani,
he received the blow of which his face bore the marks to
his dying day.
Though Michelangelo's earliest studies were directed
towards painting, he was by nature and predilection much
more inclined to sculpture. In that art he presently
received encoivagement and training under the eye of
an ■ illustrious patron, Lorenzo dei Medici. On the
recommendation, it is said, of Ghirlandaio,. he was trans-
ferred, before the term of his Apprenticeship as a painter
had expired, to the school of sculpture established by
Lorenzo in the Medici gardens. Here he could learn to
match himself against his great predecessor, Donatello, one
of *hose pupils was the director of the school, and to com-
pare the works of that maittr and his Tuscan contemporaries
with the antiques collected for th« instruction of the scholars.
Here, too, he could listen to discourses on Platonism, and
steep himself in the doctrines of an enthusiastic philosophy
which sought to reconcile wth Christian faith the lore and
the doctrines of the Academy. Michelangelo remained a
Christian Platonist to the end of his days ; he was also
from his youth up a devoted student of Dante. His
powers of mind and hand soon attracted attention, and
secured him the regard and favour of his patrons in spite
of his rugged, unsociable exterior, and of a temper which,
at best was but a half-smothered volcano.
Michelangelo had been attached to the school and house-
hold of the Medici for barely three years when, in 1492,
his great patron Lorenzo died. Lorenzo's son Piero dei
, Medici inherited the position, but not the qualities, of his
father ; Florence soon chafed under his authority ; and
towards, the autumn of 1494 it became apparent that
disaster was impending over him and his adherents.
Michelangelo was constitutionally subject to dark and
sudden presentiments : one such seized him now, and,
without awaiting the popular outbreak which soon followed,
he took horse with two companions and fled to Bologna.
There, being now in his twentieth year, he was received with
kindness by a member of the Aldovrandi family, and on
his commission executed two figures of saints, and one of
an angel, for the shrine of St Dominic in the church of St
Petronius. After about a year, work at Bologna failing,
and his name having been included in his absence on the
list of artists appointed to provide a new hall of assembly
for the Gteat Council of Florence, ilichelangelo returned
home. The strange theocracy established by Savonarola
was now in force, and the whole character of civic life at
Florence was for the time being changed. But Michelangelo
was not left without employment. He found a friend in
another Lorenzo, the son of PLerfrancesco dei Medici, for'
whom he at this time executed a statue of the boy St John.
Having also carved a recumbent Cupid in imitation of the
antique, it was suggested to him by the same pUtron
that it should be so tinted and treated as to look like a
real antique, and sold accordingly. Without increasing-
the price he put upon the work, Michelangelo for amuse-
ment lent himself to the counterfeit, and the piece was then
actually sold for a large sum to a Roman collector, the
cardinal San Giorgio, as a genuine work of antiquity, — the
dealer appropriating the profits. AVLen presently the
cardinal discovered the fraud, he caused the dealer tn
refund ; but as to Michelangelo himself, it was represented
to the young sculptor that if he went to Rome, the amateur
who had just involuntarily paid so high a tribute to his
skill would certainly befriend him. He set forth accord-
ingly, and arrived at Rome for the first time at the end of
June 1496. Such hopes as he may have entertained of
countenance from the cardinal San Giorgio were quickly
dispelled. Neither did the banished Piero dei Medici, who
also was now living at Rome, do anything to help him.
On the other hand Michelangelo won the favour of a
Roman nobleman, Jacopo Galli, and tluough him of the
French cardinal Jean de Villiers de la Grolaie, abbot of
St Denis. From the former he received a commission for
a Cupid and a Bacchus, from the latter for a Pitlti, or
JIary lamenting over the body of Christ, — works of which
probably all three, the last two certainly, are preserved.
Michelangelo's stay in Rome at this time lasted five
years, from the summer of 1496 till that of 1501. The
interval had been one of extreme political distraction at
Florence. The excitement of the French invasion, the
mystic and ascetic regimen of Savonarola, the reaction
which led to his overthrow, and finally the external wars
and internal dissidences which preceded a new settlement,
had all created an atmosphere most unfavourable to art.
230
MICHELANGELO
Nevertheless Ludovico Buonarroti, who in the troubles of
149-t had lost a small permanent appointment he held in
the customs, and had come to regard his son Michelangelo
as the mainstay of his house, had been repeatedly urging
him to come home.
A spirit of family duty and family pride was the ruling
principle in all Michelangelo's conduct. During the best
years of his life he submitted himself sternly and without
a murmur to pinching hardship and almost superhuman
labour for the sake of his father and brothers, who were
ever selfishly ready to be fed and helped by him. Having
now, after an illness, come home in 1501, ilichelangelo
received the request from the cardinal Francesco Picco-
lomini to adorn with a number of sculptured figures a
shrine already begun in the cathedral of Siena in honour
of the most distinguished member of his house. Pope
Pius n. Four only of these figures were ever executed,
and those not apparently, or only in small part, by the
master's hand. A work of greater interest in* Florence
itself had diverted him from his engagement to his Sienese
patron. This was the execution of the famous colossal
statue of David, popularly known as the Giant. It was
carved out of a huge block of marble on which another
sculptor, Agostino d'Antouio, had begun unsuccessfully to
work forty years before, and which had been lying idle
ever since. Michelangelo had here a difficult problem before
him. Without much regard to tradition or the historical
character of his hero, he carved out of the vast but cramped
mass of material a youthful, frowning colossus, which
amazed every beholder by its freedom and science of execu-
tion, and its victorious energy of expression. All the best
artists of Florence were called in council to determine on
what site it should be set up, and after much debate the
terrace of the Palace of the Signory was chosen, in prefer-
ence to the neighbouring Loggia dei Lanzi. Here accord-
ingly the colossal David of Michelangelo took, in the month
ni May 150-1, the place which it continued to hold ever after-
wards, until ten years ago, in 1873, it was removed for
the sake of protection to a hall in the Academy of Fine
Arts. Other works of sculpture by the same indomitable
hand also belong to this period : among these another
David, in bronze, and on a smaller scale ; a great rough-
hewn St Matthew begun but never comjileted for the
cathedral of Florence ; a Madonna and Child executed on
the commission of a merchant of Bruges ; and two un-
finished bas-reliefs of the same subject.
Neither was Michelangelo idle at the same time as a
painter. Leaving disputed works for the moment out of
sight, he in these days at any rate painted for his and
Raphael's common patron, Angelo Doni, the Holy Family
now in the Uffizi at Florence. And in the autumn of
1504, the year of the completion of the David, he received
from the Florentine state a commission for a work of
monumental painting on an heroic scale. Leonardo da
Vinci had been for some months engaged on his great
■cartoon of the Battle of Anghiari, to be painted on the
wall of the great hall of the municipal council. The
gonfaloniere Soderini now procured for Michelangelo the
commission to design a companion work. Michelangelo
chose an incident of the Pisau war, when the Florentine
soldiery had been surprised by the enemy in the act of
bathing : he da.shed at the task with his accustomed fiery
energy, and had carried a great part of the cartoon to
co.mpletion when, in the early spring of 1 50.5, he broke off
the work in order to obey a call to Rome which reached
him from Pope Julius 11. His unfinished cartoon showed
how greatly Michelangelo had profited by the example of
his elder rival, Leonardo, little as, personally, he yielded
to his charm or could bring himself to respond to his
courtesy ._^The ^work of Michelangelo's youth is for the
most part comparatively tranquil in character. His early
sculpture, showing a degreq of science and perfection un-
equalled siuce the antique, has also something of the
antique serenity. It bears strongly the stamp of intel-
lectual research, but not by any means that of storm or
strain. In the cartoon of the Bathers, he on the other
hand appropriated and carried farther the mastery, which
Leonardo had first asserted, over every variety of violent
action and every e.xtreme of energetic movement. In it
the qualities afterwards proverbially associated with
Michelangelo — his furia, his terribilita, the tempest and
hurricane of the spirit which accompanied his unequalled
technical mastery and knowledge — first found expreesion.
With Michelangelo's departure to Roiuo early in 1505 the first
part of his artistic career may be haid to end. It will be convenient
here to recapitulate its principal results in sculpture and paiating,
both those preserved, and those recorded but lost.
SuuLPTi-RE.— Floreuce, 1489-94. Head of a Faun, National
Sluseum, Florence (?). Condivi describes llichelangelo's fin-t essay
in sculpture as a head of an agedfauu with a front tooth knocked oof,
this latter point having been an afterthought suggested by Lorenzo
dei Medici. The head is commonly identiticd with one in the
National Museum at Florence, which, however, bears no marks of
Michelangelo's style, and is in all probability spurious. Madamui
ScaUd on a SUp, Casa Buonarroti, Florence. This bas-relief is a
genuine example of Michelangelo's early work in the Medicean
school under Bertoldo. It is executed in low relief in imitation of
the technical style of Donatello; but the attitudes and diaracteni
of the figures, and tlie long-drawn, somewhat tormentKi folds oi
drapery, recall ratlier the manner of Jacopo deila Qaercia. Cen-
tauromacJtia, Casa Buonarroti. A fine and unqv'.fstionably geniiine
work in full relief, of probably somewhat later date than the last-
mentioned ; Midielangelo has followed the anti-jue in his con-
ception and trtatinent of the nude, but not at all in thearrange-
, mcnt of the subject, which occurs frequently in works of ancient art.
Bologna, 14i'4-95. Kneeling Angel, supporting the shrine of
St Dominic. This is the figure, with crisp hair, short resolute
features, and ilmpcry clinging to show the limbs, on the right-
hand side of the spectator as he fronts the altar. The prettier
and more engiging figure at tlie opposite end was long taken to
be Michelangelo's work, but is really that of Niccolo dell' Area.
iliclielangelo also finished the figure of St Petronius on the cornice
of the same altar, begun by the same KiccoM, and executed one of
St Proculus whicli has perished.
Florenco, 1495-96. SI John in the If'iMerness, Berlin Museum.
During the year between Slichelangclo's return from Poloinia and
his first departure to Rome he executed, as has been narrated above,
a stcitue of S. Giovannino for Lorenzo di PieriVanccsco dei Medici.
This hal for centuries been supposed lost, when in 1874 it wu
declared to have been found in the possession of Count Gualandi-
Rossalmiui at Pisa. Vehement and prolonged discussions arose
as to the authenticity of the work, and at last it w-as bought for
the Berlin Museum, where its genuiuencss is with apparently good
reason maintainetl. The stripling saint stands naked but lot a
skill about his loins, liolding a honeycomb in his left hand and
lifting to his mouth a goat s horu full of honey with his right
ru^sloriUion of an antique grmtp of Bacehns and Aniythis, Lflizi
Galiery, Florence. This interesting restoration of an antique torso,
by the'addilion of a head, the lower part of the legs, and tlie accessory
figure of an attendant genius, a iilintli, and mask, is not one of the
works traditionally ascribed to Michelangelo; but has lately, and
as it seems rightly, been claimed for hiiu on internal evidence.
Heeiimbcnt Cupid, bought by the cardinal San Giorgio as an
antique. Tliis work, which played an important part in Michel-
angelo's history, is unfortunately lost.
Rome, 1495-1501. Kneeling CuinJ, South Kensington Museum,
London. This beautiful statue of an athletic youth kneeling on
the right knee, looking over his right shoulder, with tho right
hand lowered and the left raised, and having a quiver on the
ground beside him, is acknowledged on internal grounds aa an
early work of Michelangelo. There is sonic ambiguity about the
character and action of the pei-soimM; but the work is usutUj
identified with tho Cupid which Michelangelo is rcconled to have
ctecntcd at this time for Jacoiw Galli. B^ieehus ami Young FaiiH,^
National Museum, Florence. 'This is uiinnestionably the " Bacchus"
commissioned by tho same patron. The finely-framed but soft-
limbed youthful gotl, his weight sufiwrted somewhat staggeringly
on the left leg, holds up a wine cup in his right hand, and with his
loosely-hanging loft hand holds a cluster of gia|)cs, at whicli a
child-faun sUnding a little behind him grasps and nibbles. The
surface highly finished aud polished, as in the Berlin St .lohn.
I'ir^in Lamenting Ihi Dead Chrial, St Peter's, Rome. This groOD,
eieculcd for tho French abbot of St Denis, is the finest of ill
MICHELANGELO
231
IlicheUngelo's eavly sculptures, and one of the finest of liis life.
It still recalls the ideals of some of the earlier Tuscan roasters,
especially Jacopo da Quercia ; but the execution is of a mastery
and nobility unprecedented in Italian art. The Virgin, in drapery
of magnificent design, with her left kneo somewhat raised and her
right hand slightly extended, sits holding on her lap the dead
Christ,— a figure of splendid frame and modelling as well as of
admii-able pathos and dignity in expression.
Florence, 1501-6. Four Sainls decorating the Shrine of Pius U. ,
in the cathedral of Siena. These figures represent the. only part
which Michelangelo ever completed of his contract with the car-
dinal Piecolomini and his heirs. They are evidently carried out by
the liand of pupils only. Vinjin and Child, Liebfraucnkirche,
KvUges. This pleasing group has been since the days of Albert
Uiircr attributed to Michelangelo, and bears the manifest stamp
<)1 liis design, though its execution may be partly by inferior
hands. It is placed close to the tombstone of a member of the
Mosoheroni (or Moskeflon) family. We know that Michelangelo
executed at this time, for one'of this very family, a work which the
ancient biographers describe as having been in bronze, — a medal-
lion in that metal, says explicitly Vasari ; but it is probably really
the marble "roup, in question. Virgin and Child, Royal Academy,
London. Tnis beautiful unfinished circular relief is identified with
ono recorded to have been executed by the master for Taddeo
Gaddi. Virgin and Child, National Jlusenm, Florence,— a similar
iclief, also unfinished, originally ordered by Bartolommeo Pitti.
Youthful David, Academy of Arts, FloMuce. Of this colossal
work, which in spite of its scale and subject has still, in grace
of pose and style, a considerable artistic afiiuity with the earlier
Bacchus and St John, enough has been said. Figure of David,
a small statue in bronze. Several extant works have been pointed
out as probably identical with this lost statue ; but the claims of
r.cne have been generally acknowledged.
Painting. — Holy Family, Uffizi, Florence. This circular picture,
painted for Angelo Doni, and mentioned by the earliest biographers,
IS the only perfectly well-attested panel-painting of Michelangelo
which exists. His love of restless and somewhat strained actions is
illustrated by the action of the Madonna, who kneels on the ground
holding up the child on her right shoulder ; his love of thonudo
by the introduction (wherein he follows IjUca Signorclli) of some
otherwise purposeless undrapcd figures in the background. Virgin
Olid Child with Four Angels, National Gallery, London. This
unfinished painting, marked by great grace as well as severity of
feelingand design, was formerly attributed to Domenico Ghirlandaio,
but is now commonly held to bo the earliest extant picture by Michel-
angelo, Ofhisraanner, especiallyinthedosignand treatment of the
drapery, it bears evident marks ; but the execution seems like that
of some weaker pupil or companion, perhaps Ridolfo Ghirlandaio
or Granacci. EntombTiiint of Christ, National Gallery, Loudon.
This picture, also unfinished, has in like manner been much con-
tested. Its composition is unfortunate ; weaker hands have dis-
figured some portions of the work ; but the extraordinary excellence
of other portions, and the grandeur of some of the actions,
render it probable that the work is one begun and afterwards
abandoned by Michelangelo himself. Cartoon of the Battle of
Anghiari. Of this famous lost work (begun, though apparently
not completed, in the period now engaging us) the only authentic
record is contained in two early engravings, one by ilarcantoiiio
and the other by Agostino Vencziano. An elaborate drawing of
many figures at Holkham Hall, well known and often engraved,
seems to be a later £cnto destitute of real authority'.
Slicneiangeto iiaa not Deen iong in Koine betore Popo
Juliws devised fit employment for him. That capacious
and headstrong spirit, on fire with great enterprises, had
conceived the idea of a sepulchral monument to com-
memorate his glory when he should be dead, and to be
executed according to his own plans while he was Still
living. He entrusted this congenial task to Michelangelo.
The design being approved, the artist spent the winter of
1.50-5-6 at the quarries of Carrara, superintending tlic
excavation and shipment of the necessary marbles. In the
spring ho returned to Rome, and when the marbles arrived
fell to with all his energy at the preparations for the work.
For a while the pope followed their progress eagerly,
and was all kindness to the young sculptor. But presently
his_ disposition changed. In Michelangelo's absence an
artist who was no friend of his, Bramante of Urbino, had
been selected by Julius to carry out a new architectural
sq^eme, commensurate with the usual vastness of his con-
ceptions, namely the rebuilding of St Peter's church. To
the influenco .;nj the malice of r.rd]i:-.mtj '.Michclange'o
attributed the unwelcome invitation he now received to
interrupt the great work of sculpture which he had just
begun, in order to decorate the Sixtine chapel with frescos.
Soon, however, schemes of war and conquest interposed. to
divert the thoughts of Julius, not from the progress of his
own monument merely, but from artistic enterprises
altogether. One day Michelangelo heard him say at table
to his jeweller that he meant to spend uo more money on
pebbles' either small or great. To add to the artist's dis-
comfiture, when he went to apply in person for paymeuts
due, he was first put off from day to day, and at last
actually, with scant courtesy dismissed. At this his dark
mood got the mastery of him. Convinced that not his
employment only but his life was threatened, he suddenly
took iorse and left Rome, and before the messengers of
the pope could overtake him was safe on Florentine
territory. Michelangelo's flight took place in April 1506.
Once amoiig his own people, he turned a deaf ear to all
overtures made from Rome for his return, and stayed
throughout the summer at Florence, how occupied we are
not distinctly informed, but apparently, among other
things, on the continuation of his great battle cartoon.
During the same summer Julius planned and executed
the victorious military campaign which ended in his
unopposed entry at the head of his army into Bologna.
Thither, under strict safe-conduct and promises of renewed
favour, Michelangelo was at last prevailed on to betake
himself. Julius received the truant artist kindly, as indeed
between these twa volcanic natures there existed a natural
affinity, and ordered of him his own colossal likeness in
bronze, to be set up, as a symbol of his conquering
authority, over the principal entrance of the church of St
Petronius. For the next fifteen months Michelangelo
devoted his whole strength to this new task. The price
at which he undertook it left him, as it turned out, hardly
any margin to subsist on. Jloreover, in the technical art
of metal casting he was inexperienced, and an assistant
whom he had summoned from Florence proved insubor-
dinate and had to be dismissed. Nevertheless his genius
prevailed over every hardship and difficulty, and on the
21st of February 1508 the maje.^tio bronze colossus of
the seated pope, robed and mitred, with one hand grasping
the keys and the other extended in a gesture of benedic-
tion and command, was duly raised to its station over the
church porch. Three years later it was destroyed in a
revobition. The people of Bologna rose against the
authority of Julius ; his delegates and partisans Were cast
out, and his effigy hurled from its place. The work of
Michelangelo, after being trailed in derision through the
streets, was broken up and its fragments cast into the
furnace.
Meanwhile the artist himself, as soon as his work was
done, had followed his reconciled master back to Rome.
The task that here awaited him, however, was after all not
the resumption of the papal monument, but the execution
of the series of paintings in the Sixtine chapel which had
been mooted before his departure. Painting, he always
averred, was not his business; and he entered with
mi-sgiving and reluctance upon his new undertaking.
Destiny, however, so ruled that the work thus thrust upon
him remains his chief title to glory. His history is one of
indomitable will and atoiost superhuman energy, yet of will
that hardly ever had its way, and of energy continually
at war with circumstance. The only work which in all his
life he was able to complete as he had conceived it was
this of the decoration of the Sixtine ceiling. The pope
had at first proposed a scheme including figures of the
twelve apostles only. Michelangelo would be content with
nousht so meacre, and furnished in.steod a design of many
huiidrtd tigureX Lmbovlyi'i- all ih-i lii.^lory oi creation and
232
MICHELANGELO
of the first patriarchs, with accessory personages of prophets
and, sibyls dreaming on the new disi>ensation to come, and,
in addition, those of the forefathers of Christ. The whole
was to be enclosed and di\'ided by an elaborate framework
of painted architecture, with a multitude of nameless human
shapes supporting its several members or reposing among
them, — shapes mediating, as it were, between the features
of the inanimate framework and those of the great dramatic
and prophetic scenes themselves. Michelangelo's plan was
accepted by the pope, and by !May 150S his preparations
for its execution were made. Later in the same year he
summoned a number of assistant painters from Florence.
Trained in the traditions of the earlier Florentine school,
they were unable, it seems, to interpret Michelangelo's
designs in fresco either with sufficient freedom or sufficient
uniformity of style to satisfy him. At any rate he soon
dismissed them, and carried out the remainder of his
colossal task alone, except for the necessary amount of
ptirely mechanical and subordinate help. The physical
conditions of prolonged work, face upwards, upon this vast
expanse of ceiling were adverse and trying in the extreme.
But after four and a half years of toil the task was
accomplished. Michelangelo had during its progress been
harassed alike by delays of payment and by hostile intrigue.
The a'osolute need of funds for the furtherance of the
undertaking had even constrained him at one moment to
break off work, and pursue his inconsiderate master as far
as Bologna. His ill-wishers at the same time kept casting
doubts on his capacity, and vaunting the superior powers
of Raphael. That gentle spirit would by nature have been
no man's enemy, but unluckily Michelangelo's moody, self-
concentrated temper prevented the two artists being on
terms of amity .such as might have slopped the moutlis of
mischief-makers. Once during the progress of his task
Michelangelo was compelled to remove a portion of the
Bcaflolding and exhibit what had been so far done, when
the effect alike upon friends and detractors was overwhelm-
ing. Still more complete was his triumph when, late in
the autumn of 1512, the whole of his vast achievement
was disclosed to view.
The main field of the Sixtino ceiling is diviJeJ into four larger
alternating with five smaller fields. . The following is the order of the
subjects depicted in them; — (1) the dividing of the light from tlie
darkness; (2) the creation of sun, moon, and stars, and of tlie
herbage ; (3) the creation of the waters ; (4) the creation of man ;
(6) the creation of woman ; (6) the temptation and expulsion ;
(7) an enigmatical scene, said to represent the sacrifice of Cain and
Abel, but rather resemhlin" the sacrifice of Noah ; (8) tlie deluge ;
(9) the drunkenness of Noah. The figures in the last tliree of thc=e
scenes are on a smaller scale than those in the first six. In numbers
), 3, 5, 7, and 9 the field of the picture is reduced by the encroach-
ments of the architectural framework and supportei-s. These sub-
jects are flanked at each end by the figure of a seated prophet or
sibyl alternately; two other prophets are introduced at each ex-
tremity of the series, making seven prophets and five sibyls in all. In
the angles to right and left of the prophets at the two extremities
are the Death of Goliath, the Death of Judith, the Brazen Ser-
pent, and the Panishment of Haman. In the twelve lunettes
above the windows, and the similar number of triangular vaulted
spaces over them, are mysterious ponj>s, or pairs of groups, of
figures, which from Michelangelo's own time have usually been
known as Ancestors of Christ, The army of nameless architectural
and subordinate figures is too numerous to bo liero spoken of.
The work represents all the powers' of Michelangelo at their best.
Disdaining all the accessory allurements of the painttr's att, he
has concentrated Itimself upon the exclusive delineation of the
human form and face at their highest power. His imagination
lias conceived, and his knowledge and certainty of hand have enabled
liim to realize, attitudes and combinations of unmatched variety
and grandeur, and countenances of unni.itched expressiveness anil
power. But^e has not trusted, as he came later to trust, to science
and acquired knowledge merely, neither do his personages, so far
as they did r ftcrwards, transcend human possibility or leave the
fact.s of actual life behind them. In a word, his sublimity, often
in excess of the occasion, is here no more than equal to it ; more-
over,it is combined with the noblest clemonts of grace and even of
tcndernosa. As for the intellectual meanings of his vast design,
I over and above those wliieh reveal thf msflvrs ,it a first glance or
by a bare description, — they are from the nature of the case in-
I exhaustible, and c;cn never be perfectly defined. 'WhateTer the
( soul of this great Florentine, the spiritual heir of Dante, with
I the Christianity of the Jliddle Age not shaken in hia mind, but
expanded and transccndentalized, by the knowledge and love of
Plato, — whatever tiie soul of such a man, full of suppressed tA.*nder-
ness and righteous indignation, and of anxious questionings of
coming fate, eould conceive, that Michelarigelo has expressed or
shadowed forth in this great and significant scheme of paintings.
The details it must remain for every fresh student to interpret in
his own manner.
The SLxtine chapel was no sooner completed than
Michelangelo resumed work upon the marbles for the
monument of Julius. But four n-.onths only had passed
' when Julius died. His heirs immediately entered (in the
I summer of 1513) into a new contract with Michelangelo
I for the execution of the monument on a reduced scale.
1 VfUat the precise nature and extent of the original design
I had been "n'e do not know, but the new one was extensive
and magnificent enough. It was to consist of a great
quadrilateral structure, two courses high, projecting from
the church wall, and decorated on its three unattached side«
with statues. On the upper course was to be placed the
colossal recumbent figure of the pope under a canopy,
and beside it mourning angels, with prophetic and
■ allegoric personages at the angles, — sixteen figures in
I all. The lower course was to be enriched with twenty-
four figures in niches and ou projecting pedestals : — ia
! the niches. Victories trampling Ou conquered Provinces:
I in the pedestals, Arts and Sciences in bond, ^.e. The
I entire work was to be completed in nine years' time.
During the next three years, it would seem, Michelangelo
j brought to completion three at least of the promised
figures, and they arc among the most famous of all exist-
ing works of the sculptor's art, — namely, the Moses now
in the church of S. Pietro in Vincoli at Rome and the
two " Slaves " at the Louvre.
The Moses, originally intended for one of the angles of the upper
course, is now placed at the level of the eye, in the centre of the
princip.^1 face of the monument as it was at last finished, on a
deplorably reduced and altered scale, by Michelangelo and his
assistants in his old age. The prophet, heavily bearded and dniped,
with, only his right arm bare, sits with his left foot drawn back,
his head raised and tumed to tlie left with an expression of in-
digiintipn and menace, his left hand laid on his lap and his right
grasping tho tables of the law. The work, except in one or two
places, is of the utmost finish, and the statue looks like one of the
prophetsof the Sixtineccilin" done iu marble. The " Slaves " at
the Louvre are youthful male figures of e<tual)y perfect execution,
nude but for the band which passes over tlie breast of one and the
right leg of the other. One, w-ith his left hand raised to l;is head
and his right prc-^sed to his boscm, and his tyes almost closed,
seems succumbing to the agonies of death ; the other, with his arms
bound behind his back, looks upward still hopelessly struggling.
There is reason to believe that all three of these figures were finished
between 1613 and 151G. The beginnings of other figures or groups
intended for the same monument are to !'« found at florenco, \vhero
they were no doubt made and then abandoned some years h'.ter, —
viz., four rudely blocked figures of slaves or prisonore, in a grotto
of the Boboli gardeis, and the sc-eallcd Victory in the National
Museum, an unfinished gioup of a conil)atant kneeling on and
crushing to death a fallen enemy; with tliesc may be associated
a wax model known us Hercules and Cacus in the South Keo-
sington Museum, aud the figure of a crouching man at St Peters-
burg.
By this time (1516) Michelangelo's evil star was again
in the ascendant Julius IL had been succeeded on the
papal throne by a Medici under the title of Leo X. The
Medici, too, had about the tame time by force and fraud
re-established their sway in Florence, overthrowing the free
institutions that had prevailed there since tho days of
Savonarola. Now un the one hand this family .jvcrc the
hereditary friends and patrons of Michelangelo; on the
other hand he was a patriotic son of republican Florence;
60 that henceforward his personal allegiance and his
political Eympatliies were destined to be at conflict. Over
MICHELANGELO
233
much of bis art, a-s has been thought, ttie pain and per-
plexity of this conflict have cast their shadow. ;. For the
present the consequence to him of the rise to power of the
Medici was a fresh interruption of his cherished work on
the tomb of Julius. Leo X. and his kinsmen insisted that
Jlichelangelo, regardless of all other engagements, must
design and carry out a great new scheme for the- enrich-
ment of their own family church of San Lorenzo in
Florence. The heirs of Julius on their part showed an
accommodating temper, and at the request of Leo allowed
their threeyears'-old contract to be cancelled in favour of
another, whereby the scale and sculptured decorations of
the Julian monument were again to be reduced by nearly
a half.^ Unwillingly Michelangelo accepted the new com-
mission thus thrust upon him for the churcli facade at
Florence; but, having once accepted it, he produced a
design of combined sculpture and architecture as splendid
and ambitious in its way as had been that for the monu-
ment of Julius. In the summer of 151C he left Rome for
Carrara to superintend the excavation of the marbles.
Michelangelo was now in his forty-second year. Though
more than half his life was yet to come, yet its best
days had, as it proved, been spent. All the hindrances
■which he had encovmtered hitherto were as nothing to
tliose wliicli began to beset hun now. For the supply of
materials for the fagade of San Lorenzo he had set a firm
of masons to work, and had himself, it seems, entered into
a kind of partnership with them, at Carrara, where lie knew
the quarries well, and where the industry was hereditaiy
and well understood. AVhen all was well in progress there
under his own eye, reasons of state induced the Medici
and the Florentine magistracy to bid him resort insti,a<J
to certain new quarries at Pietrasanta, near Serravallc in
the territory of Florence Hither, to the di.sgust of liis olil
clients at Carrara and to his own, Michelangelo accordingly
had to transfer tlfe scene of his labours. Presently he found
himself so innicJed and enraged by the mechanical difficulties
of raising and traiisi>orting the marbles, and by the disloyalty
and incompetence of tlioac with whom he Jiad to deal, that
he was fain to throw up the commission altogether. Tlie
contracts for the fa^^ade of San Lorenzo were rescinded in
Jlaroh 1518, and the whole magnificent sdieme came to
notliing. "Michelangelo then returned to Florence, where
proposals" of work pouied in oii him from many quarters.
The king of France desired sometliing from his liand to
place Wsidc the two pictures he possessed by Raphael.
The authorities of Bologna wanted liim to design a fai;adc
for their cliurch of St IVtnmiti.s ; those of Genoa to ca.~t a
Btatuc in bronze of their gnat comniamler, Andrea Doria.
Cardinaljjrimani begged hard for any (Mcturo or s(atue he
might have to tparc ; other amateurs importuned him for
so much as a pencil drawing or sketch. Lastly his friei\d
and partisan Sebastian del I'lombo at Rome, ever eager to
keep ui> the feud between the followers of Midielangelo
and'those of Rapliael, be>ouglit him on Raphael's death to
return at once to liomc, and take out of the hands of the
dead master's pupiU the works of painting still remaining
to be done inihe S'atican chamlicrs. Michelangelo complied
with none of these requests. All that wc know oT hi* iloing
at this.timc was the finishing a connnission received iind
first put in liand fovu' years previously, for a full-sized
Btatue of a nude Christ grasi.ing the Cross. This statue,
completed and sent to Rome in l'>21 (with some List touches
added by su'iordinatc. hands in Rome itself), stands now in
the cliurch of Sta Maria soiira Minerva ; there is little in
it of the Christian spirit as commonly nn.lcrstood, although,
ill those parts which MicIielangL-Ki liinisvlf finished, there
is extreme accoiiipli>limeiit of desi'.;n ami workmanship.
■Jlicncxt twclNC years of Mi.helangilo.s life (l.")-2-2-:ll)
were spent at Florence, and again emiiloyeU'priucipally iu
the service of his capricious and ancongenial patrons, the
Medici. The plan of a great group of monuments to
deceased members of this family, to be set up in their
mortuary chapel in San Lorenzo, seems to have been formed,'
and preparations to have been made by Jlichelangelo for
its execution, as early as 1519. It was not, however, until
1524, after Leo X. had died, and his successor Adrian VI.
had been in his turn succeeded by another Medicean pope,
Clement VII., that any practical impulse was given to the
work. Even then the impulse was a wavering one. First
Clement proposed to associate another artist, Sansavino,
with Michelangelo in his task. This proposal being on
Michelangelo's peremptory demand abandoned, Clement
next distracted the artist with an order for a new archi-
tectural design, — that, nimely, for the proposed Jledicean
or " Laurentian " library. When at last the plans for the
sepulchral monuments took shape, they did not include, aa
had been at first intended, memorials to the founders of
the house's greatness, Cosimo and Lorenzo the JIagnificent,'
or even to Pope Leo X. himself, but only to two younger
members of the house lately deceased, Giuliano, duke of
Nemours, and Lorenzo, duke of Urbino. '< Michelangelo
biooded,long over his designs for this work, and was still
engaged on its execution — his time being partly also taken'
up by tlie building jilans for the Medicean library-r-when
political revolutions interposed to divert his industry," .In
1527 came to pass the sack of Rome by the AustriansJ
and the apparently irretrievable ruin of Pope Clement.^ ,The
Florentines seized the occasion to expel the Medici from
their city, and sot up a free republican government ^once
more. Naturally no more funds for the work; in -San
'!,o''enzo were forthcoming, and Michelangelo, on the
invitation of the new signory, occupied himself for a
«liilo with designs for a colossal group of Samson and
the Pliilistines, to be wrought out of a block of marble
which Irad been rough-hewn already for another purpose
by Baccio Bandinelli. Soon, however,, he .was called to
help in defending the city itself from danger. Clement and
his enemy Charles V. having become reconciled, both alike
were now bent on bringing Florence again under the nUe of
tlie Medici. In view of the approaching siege, Michelangelo
was a]i]>ointed engineer-in-chief of the fortifications. He
spent the early summer of 1529 in strengthening the
defences of San Miniato ; from Ju.ly to September he waa
absent on a diplomatic mission to Ferrara and Venice.
Returning in the middle of the latter month, he found the
cause of Florence hopeless from internal treachery and
from the overwhelming strength of her enemies. One of
his dark seizures overcame him, and he departed again
suddenly for A'enice. Not cowardice, but despair of his
(rity's liberties, and still more of his own professional pro-
spects amid the turmoil of Italian affaii's, was the motive
of his departure. For a while he remained in Venice,
negotiating for a future residence in France. Then, while
the siege was still in progress, he returned once more to
Florence ; but in the final death-struggle of her hbeHies he
bore no part. When in 1530 the city submitted to her
conquerors, no mercy, was shown to most of those who had
taken part in her defence. Michelangelo believed himself
in danger with the rest, but on the intervention of Baccio
Valori he was jircscntly taken back into favour and
employment by Pope Clement. For three years more he
still remained at Florence, engaged princiimlly on the cotH-
I'letionof tlic Medici monuments, and on the continuance of
the Medicean library, but partly also, oil a picUire of»Led^
for the duke of Ferrara. '"
Til.- sintii.-i nf tlic McJii-i inoniimont taKc rank licsiilo the Mose«
.111.1 till- Slaves ns tin: liu.-st work of iliiliobnsdo's central. tima
ill >cul|.tiiu- ; moi.ovcr. tlinudi some of t*c n.:;iiics .ire uufiaisliecl,!
tlipv coualiiulc as iKtu:illy executed a coiiq'Klo sclicnie. TUey
XVI. — 30
234
Yi I C H E L A X G K L O
:onsist of a Kadonns and Child (left impeifect because the marble
was short in bulk), and of tlie two famous monumental groups, each
consisting of an armed and seated portrait-statue in a niche, with
two emblematic figures reclining on each svle of a sarcophagus
below. The portraits are treated not realistically but typically. In
that of Lorenzo seems to be typified the mood of bi-ooding and
concentrated inward thought preparatory to warlike action ; in
that of Giuliano, llie type of alert and confident practical survey
immediately preceding the moment of action. To this contrast of
the meditative and active characters coiTesponds to some ext^it a
^contrast in the emblematic groups accompanying the portraits. At
the feetof the Duke Giuliano recline the shapes of Night and Day, —
Ithe former a female, the latter a male personification, — the former
fiunk in an attitude of deep but uneasy slumber, the latter (whoso
head and face are merely blocked out of the marble) lifting himself
ftn one of wrathful and disturbed awakening. But for Michelangelo's
(unfailing grandeur of style, and for the sense which his works con-
,vey of a compulsive heat and tempest of thought and feeling in the
iGoul that thus conceived them, both these attitudes might be charged
jwith extravagance. As grand, but far less violent, are those of the
two companion figures that recline between sleep and waking on
the sarcophagus of the pensive Lorenzo. Of these, the male figure
is known as Evening, and the female as Morning {Crcpitscolo and
'Aurora). In Michelangelo's origiual idea, figures of Earth and
Heaven were to be associated with those of Night and Day on the
monument of Giuliano, and others of a corresponding nature, no
doubt, with those of the Sloming and Evening Twilight on that of
Lorenzo ; these figures afterwards fell out of the scheme. Michel-
angelo's obvious and fundament.al idea was, as some words of his
own record, to exhibit the elements, and tlia powers of earth and
heaven, lamenting the death of the princes ; it is a question of
much interest, but not to be discussed here, what other ideas of
a more personal and deeper kind may have conflicted or come into
association with these, and found e.\pression in these majestic
works of art, whereof no one who looks upon them can escape the
spell.
Michelangelo had never ceased to be troubled by the heirs
and executors of Julius, as well as by his o«ti artistic con-
science and ambition, concerning the long-postponed comple-
tion of the Julian monument. Agreement after agreement
had been made, and then from the force of circumstances
broken. In 1532, on the completion of the Medicean monu-
ments at Florence, he entered into a new and what he firmly
meant to be a binding contract to complete the work, on a
scale once more very greatly reduced, and to set it up in the
church of S. Pietro in Vincoli in Rome. But once more
the demands of the pope diverted his purpose. Clement
insisted that Michelangelo must complete his decorations
of the SLxtine chapel by painting anew the great end
wall above the altar, adorned until then by frescos of
Perugino. The subject chosen was the Last Judgment,
and Michelangelo began to prepare sketches. For the
next two years he lived between Rome and Florence, and
in the autumn of 1534, in his si.xtieth year, settled finally
and for the remainder of his life at Rome. Immediately
afterwards Pope Clement died, and was succeeded by a
Farnese under the title of Paul III. Even more than his
predecessor, Paid insisted on claiming the main services of ■
Michelangelo for himself, and forced him to let all other
engagements drift. For the first seven years after the
artist's return to Rome, his time was princiiially taken up
with the painting of the colossal and multitudinous Last
Judgment. This being completed in 15-11, he was next
compelled to undertake two more great frcsco.s, one of the
Conversion of Paul and another of the Martyrdom of Peter,
in a new chapel which the pope had caused to be built in
the Vatican, an<i named after himself Capella Paolina.
The fresco of the Last Judgment in the Sixtine chapel is )>robably
the most famous single picture in the world. In it Jliclielangclo
shows more than ever tlic omnipotence of his artistic scienro, nnd
the fiery daring of liis conceptions. Tho work exhibits the
athletic unclothed human form, in every vaiiety and extremity of
hitherto unattenipted action and predicament. But of moderation,
as well as of beauty and tendcniess, it is almost entirely devoitl.
Whether from the complexion of his own thoughts, and the
8xva indigiiatio that was native to his breast, or from the influ-
ence of the passionate and embittered theological temper of the
time, Michelangelo Ims iiere neglected tho consolatory aspects of
ChriBtianity, and insisted on its terrific aspects almost c.\clusively.
Neither in the qualities of colour and execution is the work, so far
as the condition of either adinits comparison, comj-arable for charni
to the earlier and far more nobly-inspired fresf-os of the ceiling.
It is to these, and not to the Last Judgment, that the student must
turn if he would realize what is best and greatest in the art of
Michelangelo.
The frescos of the Pauline Chapel are on their part in part so
injured as to be hardly susceptible of useful study or criticism.
In their rftined state they bear evidence of the same tendencies that
made the art of Michelangelo in its latest phase so dangerous
an exaroi>le to weaker men, — tho tendency, that is, to seek for
energy and violence of action both in place and out, lor "terrible-
ness " qiuind mime, and to design actions not by help of direct
study from nature, but by scientific deduction from the abstract
laws of structure and movement. At best tbise frescos can never
have been happy examples of Michelangelo's art.
During the fifteen years (1534-49) when Michelangelo
was mainly engaged on these paintings, be had also at
last been enabled to -acquit himself, although in a manner
that can have been satisfactory to none concerned, of his
engagements to the heirs of Julius. Once more the
influence of the pope had prevailed on them to accept a
compromise altogether to their disadvantage. It we-s
agreed that the Moses executed thirty years before should
be. the central figure of the new scheme; assistants were
employed to carve two smaller flanking figures of female
personifications; and the three were in 1545 set up in 6.
Pietro in Vincoli in combination with an architectural
structure of rich but incongruous design. During tbt
same years the long-pent human elements of fervour and
tenderness in Michelangelo's nature had found vent and
utterance such as they had never found before. He had
occasionally practised poetry in youth, and there are sigas
of some transient love-passage during his life at Bologcu.
But it was not until towards his sixtieth year that the
springs of feeling were fairly opened in the heart of tbi.-
solitary, this masterful and stern, life-wearied and labou.'-
hardened man. Towards that age we find him beginning
to address impassioned sonnets, of which the sentiment is
curiously comparable to that expressed in some of Shake-
speare's, to a beautiful and gifted j outh, Tommaso Cavaheri.
Soon afterwards he made the acquaintance of the piou.s,
accomplished, and high-soulcd lady, Vittoria Colonna, widov,'
of the Marquis Pescara. For twelve years until her death,
which happened in 1547, her friendship was the greatsolacc
of Michelangelo's life. On her, in all loyalty and reverence,
he poured out all the treasures of his mind, and all his im
prisoned powers of tenderness and devotion. He painted
for her a crucifixion of extraordinary beauty, of which many
imitations but not the original have come down to us. She
was the chief inspirer of his poetry, — in which, along with
her praises, the main themes are the Christian religion, the
joys of Platonic love, and the power and mysteries of art.
Michelangelo's poetical style is strenuous and concentrated
hke the man. He wrote with labour and much self-correc-
tion ; we seem to feel him flinging himself on the material
of language with the same overwhelming energy and
vehemence, — the same impetuosity of temperament, coic-
biiied with the same fierce desire of perfection, — with
which contemporaries describe him as flinging himself en
the material of marble.
And so the mighty sculptor, painter, and poet reached
old age. An infirmity which settled on him in 1544, and
the death of Vittoria Colonna in 154", left him broken in
health and heart. But his strength held on for many a
year longer yet. His father and brothers were dead, and
his family sentiment concentrated itself on a nephew,
Leonardo, to whom he showed unremitting practical kind-
ness, coupled with his usual suspiciousness and fitfulness
of temper. In almost all his relations the old man con-
tinued to the end to manifest the same loyal and righteous
heart, accompanied by the same masterful, moody, and
estranring temper, as in youth. Aoiong the artists of
M I C — M I C
235
the younger generation he held a position ot aosolute
ascendency and authority ; nor was his example, as we
have said, by any means altogether salutary for them.
During the last years of his life he made but few
more essays in sculpture, and those not successful, but
wais much employed in the fourth art in which he ex-
celled, that of architecture. A succession of popes de-
manded his serWces for the embellishment of Eome.
For Paul III. he built the palace called after the name of
the pope's family the Farnese. On the death of Antonio
da San Gallo he succeeded to the onerous and coveted
office of chief architect of St Peter's Church, for which he
remodelled all the designs, living to see some of the main
features, including the supports and lower portion of the
great central dome, carried out in spite of all obstacles
according to his plans. Other great architectural tasks on
which he was engaged were the conversion of a portion of
the Baths of Diocletian into the church of Sta Maria degli
Angeli, and the embellishment and rearrangement of the
great group of buildings on the Roman Capitol. At length,
in the midst of these vast schemes aod responsibilities, the
heroic old man's last remains of strength gave way. He
died on the threshold of his ninetieth year, on the ISth of
February 1564.
For the bibliography of llichekngelo, which is extensive, see the
nseful though very imperfect compilation of Pasecrini, Biblior/rafia
di Michelangelo Biionarrotif kc, Florence, 1875. The most import-
ant works, taken in chronological order, are the following: — P.
Giovio, supplement to the fragmentary ZHalogits dc viris liiteris
illustribus, written soon after 1527, first published by Tiraboschi,
Sttria delta LetUralura iialiana, Modena, 1871; G. Vasari, in
Vite dfgli piit eccellenli architettori, pittori, c sntUori, &c.,
Florence, 1550; A. Condivi, Fita di Michelangelo Buonarroti^
1653; this account, for which the author, a pupil and friend of the
master's, had long been collecting materials, was much fuller than
that of Vasari, who made use of it in rewTiting his own life of
Michelangelo for his second edition, which appeared after the
master's death (1568). The best edition of Vasari is that by Mila-
nesi, Florence, 1878-83; of Condivi, that by Gori and Mariette, Pisa,
1746. The first additions of importance were published by Bottari,
Saccolta di lettcre sulta pittura, &c., Rome, 1754 (2J ed., by
Ticozzi, Milan, 1822); the next by Gaye, Carteggio incdito, 1840.
Portions of the correspondence preserved in the Buonarroti archives
were published by Guasti in his notes to the Jlimc di Michelangelo
Buonarroti, 1863, and by Daelli in Carte Michelangclesche inedite,
Milan, 1865. Complete biographies of Michelangelo had been
meanwhile attempted by J. Harford, London, 1857, and with
more power by Hermann Grimm, Lchcn Michelangelo's, Hanover
(5th ed., 1879). A great increment of biographical material
was at length obtained by the publication, in the four hundredth
year after Michelangelo's birth, of the whole body of his letters
preserved in the Buonarroti archives, — Lettcre di Michelangelo
Buonarroti, ed. G. Milanesi, Florence, 1875. This material was
first employed in a connected narrative by A. Gotti, Vita di Michel-
angelo, Florence, 1875. Next followed C. Heath Wilson, Life and
Works of Michelangelo Buonarroti, Florence, 1875, the technical
remarks in which, especially as concerns the fresco-paintings, are
valuable. Lastly, the combined lives of Michelangelo and Raphael
by Professor A. Springer in Dohme's series of KiiTist u. Kunstler,
lieipsic, 1878, contain the best biography of the master which has
yet appeared. Ot the poems of Michelangelo the best edition is
that already referred to, — G. Guasti, Bivie di Michelangelo Buonar-
roti, 1863; in earlier additions the text had been recklessly tampered
with, and the rugged individuality of the master's style smoothed
down. An edition with German translations was published by
Hasenclever, Leipsic, 1 875 ; for the English student the translations
by Mr J. A. Symonds, in Smmets of Michelangelo and Cam-
panella, London, 1878, are invaluable. (S. C.)
MICHELET, JxTLEs (1798-1874), one of the most
voluminous and remarkf.ble writers of France, and one
who only lacked a keener power of self-criticism to make
him one of the greatest, was born at Paris, August 21, 1798.
He belonged to a family which had Huguenot traditions,
and which was latterly occupied in the art of printing. His
father was a master printer, but seems not to have been
▼ery prosperous, and the son at an early age assisted him
in the actual work of the press. A place was offered him
in thd imperial printing office, but bos father was able to..
send him to the fsmions College or Lycte Charlemagne,
where he distinguished himself. He passed the university
examination in 1821, and was shortly after appointed to &
professorship or rather mastership of history in the College
Rollin. Soon after this, in 1824, he married. The period
of the Restoration and the July monarchy was one of the
most favourable to rising men of letters of a somewhat
scholastic cast that has ever been known in France, and
Michelet had powerful patrons in Villemain, Cousin, and
others. But, though he was an ardent politician (having
from his childhood embraced republicanism and a peculiar
variety of romantic free-thought), he was first of all a man
of letters and an inquirer into the history of the past.
His earliest works were school books, and they were not
written at a very early age. Between 1825 and 1827 he
produced divers sketches, chronological tables, <tc., of
modern history. His JPrecu of the subject, published in
the last-mentioned year, is a sound and careful book, far
better than anything that had appeared before it, and
written in a sober yet interesting style. In the same year
he was appointed maitre de conferences at the ficole
Normale. Four years later, in 1831, the Introduction i
t'Sistoire Universelle showed a very different style, exhibit-
ing no doubt the idiosj-ncrasy and literary power of the
writer to greater advantage, but also displaying the peculiar
visionary qualities which make Michelet the most stimulat-
ing but the most untrustworthy (not in facts, which he
never consciously falsifies, but in suggestion) of all
historians. The events of 1830 had unmuzzled him, and
had at the same time improved his prospects, and put him
in a better position for study by obtaining for him a place
in the Record Office, and a deputy-professorship under
Guizot in the literary faculty of the university. Very
soon afterwards he began his chief and monumental work,
the Ilistoire de France, which occupied him for about forty
years, and of which we shall speak presently. But he
accompanied this with numerous other works, chiefly of
erudition, such as the CEuvres Choisies dc Yico, the Memoiret
de Luther ecrits par lui-meme, the Origines du Droit
Franfais, and somewhat later the Proces des Templifrt.
1838 was a year of great importance in Michelet's life.
He was in the fulness of his powers, his studies had fed
his natural aversion to the principles of authority and
ecclesiasticism, and at a moment when the revived activity
of the Jesuits caused some real and more pretended alarm
he was appointed to the chair of history at the College de
France. Assisted by his friend Quinet, he began a violent
polemic against the unpopular order and the principles
which it represented, a polemic which made tieir lectures,
and especially Michelet's, one of the most popular resorts
of the day. He published, in 1839, a History of the
Roman Republic, but this was in his graver and earlier
manner. 'The Results of his lectures appeared in the
volumes Le Pretre, la Femme,^t la Fainille and Le Pevple.
These books do not display the apocaljijtic style which,
borrowed to a certain though no very great extent from
Lamennais, characterizes Michelet's later works, but they
contain jn miniature almost the whole of his curious cthico-
politico-theological creed — a mixture of sentimentalism,
commtmism, and anti-sacerdotalism, supported by the most
eccentric arguments, but urged with a great deal of
eloquence. The principles of the outbreak of 1848 were
in the air, and Slichelet was not the least important of
those who condensed and propagated them : indeed his
original lectures were of so incendiary a kind that the
course had to be interdicted. But when the actual revolu-
tion broke out Michelet, unlike many other men of letters,
did not attempt to enter on active political life, and merely
devoted himself more strenuously to his literary work.
, Besides continuing the great history, he undertook aud
236
M 1 C H E L E T
carried out, during the years between the downfall of LouL?
Philippe and tho {•r"^. establishment of Napoleon III., an
enthusiastic Eistoire de la Revolution Fran<;aise. Desjiite
or "because of its enthusiasm, this is by no means Michelot's
best book. The events were too near and too well known,
and hardly admitted the picturesque sallies into the blue
distance which make the charm and the danger of his
larger work. In actual picturesqueness as well as in general
veracity of picture, the book cannot approach Carlyle's ;
while as a mere chronicle of the events it is inferior to half
a dozen prosaic histories older and younger than itself.
The coup d'etat lost Michelet his place in the Eecord Office,
as, though not in any way identified with the republic
administratively, he refused to take the oaths to the
empire. But the new regime only kindled afresh his
republican zeal, and his second marriage (with Mademoiselle
Adele Malairet, a lady of some literary capacity, and of
republican belongings) seems to have further stimulated
his powers. While the history steadily held its way, a
■crowd of extraordinary little books accompanied and
diversified it. Sometimes' they were expanded versions of
its episodes, sometimes what may be called commentaries
or companion volumes. In some of the best of them
natural science, a new subject with Michelet, to which his
wife is believed to have introduced him, supplies the text.
The first of these (by no means the best) was Les Femmes
de la Revolution (1854), in which Michelet's natural and
inimitable faculty of dithyrambic too often gives way to
tedious and not very conclusive argument and preaching.
In the next, L'Oiseau (1856), a new and most successful
vein was struck. The subject of natural history was treated,
not from the point of view of mere science, nor from that
of sentiment, nor of anecdote, nor of gossip, but from that
of the author's fervent democratic pantheism, and the
result, though, as was to be expected, unequal, was often
excellent. L'Insecte, in the same key, but duller, followed.
It was succeeded by V Amour (1859), one of the author's
most popular books, and not. unworthy of its popularity,
but perhaps hardly his best. These remarkable works,
half pamphlets half moral treatise.?, succeeded each other
as a rule at the twelve months' interval, and the succession
was almost unbroken for five or six years. V Amour was
followed by La Femme (1860), a book on which a whole
critique of French literature and French character might
be founded. Then came La Mer (1861), a return to the
natural history class, which, considering the powers of the
writer and the attraction of the subject, is perhaps a. little
disappointing. The next year (18C2) the most striking
of all Micholet's minor works. La Sorcicre, made its
appearance. Developed out of an episode of the history,
it has all its author's peculiarities in the strongest degree.
It is a nightmare and nothing more, but a nightmare of
the most extraordinary verisimilitude and poetical power.
This remarkable series, every volume of which was at
once a work of imagination and of research, was not even
yet finished, but tho later volumes exhibit a certain fall-
ing oS. The ambitious £ible de rHumanite (1864), an
historical sketch of religions, has but little merit. lu La
Montagne (1868), the kst of tho natural history series, tho
tricks of staccato style are pushed even farther than by
Victor Hugo in his less inspired moment.s, though — as is
inevitable in the hands of such a master of iaiiguago as
Michelet — tho effect is frequently grandiose if not grand.
JVoi /"iTs (1869), tho last of the string of smaller books
published during the author's life, is a tractate on educa-
tion, written with ample knowledge of the facts and with
all Michelet's usual sweep and range of view, but with
visibly decUning powers of expression. But in a book
published posthumously, Le Banquet, these powers reappear
at their fullest. The picture of the indiistrious and
famishing populations of the Riviera is (■whether trun to
fact or not) one of the best things that Michelet hij dona.
To complete the hst of his miscellaneous works, two coUeo-
tions of pieces, written and partly published at different
times, may be mentioned. These are Lea Soldats de la
Revolution and Ligendcs Democraiiques du JCord.
The publication of this series of books, and the comple-
tion of his history, occupied Jlichelet during both decades
of the empire. He lived partly in France, partly in Italy,
and was accustomed to spend the winter on the Riviera,
chiefly at Hyeres. At last, in 1867, the great work of hia
life was finished. As it is now published it fills nineteen '
volumes. The first of these deals with the early 'history
up to the death of Charlemagne, tho second with the
flourishing time of feudal France, the third with the 13th
century, the fourth, fifth, and sixth with the Hundred
Tears' War, the seventh and eighth with tho establishment
of the royal power under Charles VII. and Louis XI. The
16th and 17th centuries have four volumes apiece, much
of which is very distantly connected with French history
proper, especially in the two volumes entitled Renaissance
and Riforme. The last three volumes carry on the history
of the 18th century to the outbreak of the Revolution.
The characteristics which this remarkable history shMes
with Michelet's other works will be noted presently. Afc
present it may be remarked that, as the mere division of
subjects and space would imply, it is planned on very
original principles. Michelet was perhaps the first
historian to devote himself to anything Uke a picturesque
history of the Middle Ages, and his account is still the
most vivid though far from the most trustworthy that
exists. His inquiry into manuscript and printed authorities
was most laborious, but his lively imagination, and his
strong religious and political prejudices, made him regsuxl
all things from a singularly personal point of view.
Circumstances which strike his fancy, or furnish convenient
tests for his polemic, are handled at inordinate length,
while others are rapidly dismissed or passed over altogether.
Yet the book is undoubtedly the only history of Franca
which bears the imprint of genius, and in this respect it ia
not soon likely to meet a rival.
Uncompromisingly hostile as Michelet was to tho empire,
its downfall and the accompanying disasters of the country
once more stimulated him to activity. Not only did he
wi'ite letters and pamphlets during tho struggle, but when
it was over he set himself to complete the vast task which
his two great histories had almost covered by a History of
the Kiyieteentk Centuri/. He did not, however, live to carry
it further than Waterloo, and the best criticism of it is
perhaps contained in the opening words of the introduction
to the last volume — "I'ago me presse." The new republic
was not altogether a restoration for Michelet, and his
professorship at tho ColliSge de France, of which ho con-
tended that he had never been properly deprived, was not
given back to him. Ho died at Hyircs on tho 9th of
February 1874, and an unseemly legal strife between his
representatives took place a-s to his funeral.
Tlio literary chamcteriatics of Slicliclct ore among tlio mo«t
clonrly marked and also among tlio most peculiar in F.rencU litera-
ture. A certain resemblance to Lamcnnais has been already noted,
and to this m.iy be added an occasional reminisceneeof the m.tnner
of Bossuet, But i:i the m.iin Michelet, even in tho minor d.uiUof
style, is quite original and individual. His sentences and porjgripha
are .s different as possible in construction, and rhythm from tho
orderly avhitecturo of French classic.il prose. A very frefluent
device of his (somewhat abused latterly) is ths omission of th«
verb, whiih gives the sentence the air of a continued interjection.
Elsewhere ho breaks his phr.iso, uoi linishing the repihr clans«
at all In these points and many oihcij tho rcst-mblancc to his
conteraporaty Cnrlvlo is very striking ; and, different as were
their points of view, their manners of s«cing were by no moans
unliko. llistor)- to Michelet is always pictureaquo; it is t •erics
of tiibletiis. jilusion hu b;c3 a^aij xiJo to tbt aingviUr ftf
M I (J — M i IJ
237
snective in wliiili llicsctnblcaiix aic ilj-av.ii, n jKiiii^-cUirc sn stiango
luat a reailer iuiacq\ir.iiitc»l with tlie actunl size nml icl.ilioii or tlic
objects i-eprcscntcU is ccrtiin to bo deceived. Kotbiii;:: indeed is
furtlier from Michekt's. jiuiposo tliaii deceit AlthouRli n strong
rcpubiicar., an ardent auti-sacenlotjilist, and a }iatriot of fanatical
entliusiasm, be is alwa^'S^scnijjulously fair aa far a:> Jic iindci-staiids
wbat bo is doing. Kor instance, Jiis batrcJ for England and
Englislinien is one of tbe most comically intense jiassions in litera-
tnro. He is never tired of exclaiming ogainst tlicir diabolical pride,
tlieir odious jealousy of France, their calculating covctousncss, and
sofurtlL In bis excited iinaj^iiwtion the long drama of Eurojwnii
Jiistory is a kind of conflict of Ormuzd and Ahrinian, in wbicli
Fnnicc, it is needless to say, I'lays the first jiart and England tbe
second. Yet be is never unfair to Englisb foi-titude and coolness,
never {after tbe cbildisb fashion of some of his eouutrymcn) slurs
over English victories, and often expresses genuine admiiTition
(mixetl, it is truc,'witb a shudder or twoof avei-sion) for tbe master-
ful ^-ays and constantly advancing prospcjity of tbe English iKsopIe.
So, jvitb all bis dislike to tbo priestbood, be never is chary of praise
to popo or monk wbeucver it can fairly be given, and, with ail his
rcimblicanism, be is never weary of woi-sbipping tbe heroism of a
gixai king. But his jKxjtical fashion of dealing with events, his
exaggeration of trivial incidents into great facts of history, bis fixed
ideas, especially iu reference to tbe intellectual and social condition
of media:val times, tbe evils of which bo enormously exaggei-ates,
and bis abiding prejudices of a general kind combine to distort bis
accounts iu tbe strangest fashion. A laborious person might pick
out of contcmiwrary authors a notable collection of erroneous views
of which Micbelct is not so much the author as the Buggester, for it
Is when bis brilliant exaggerations are torn from their- context and
set down in some quito other context as sober gos^icl that they are
most misleading to tliosc who do not know the facts, and most
grotesque to tliose who do. This is especially the case in regai-d to
literature. Jlichelet began his great work too early to enjoy the
benefit of the resunectiou of old French literature which has since
taken idace; and though his view of that litci-atui-c partakes of the
amorous enthusiasm v.liich colours bis view of everything French,
it is astoundingly incorrect in detail. Tbe most remarkable passage
of all perhaps is tbe passage in bis riCnai$sancc relating to Habclais,
Ronsard, and Dn Bellay, a passage so widely inconsistent not only
with sound critiiism bnt w itb historic fact that the autbor(a very rare
thing with him) makes a kind of half apology for it elsewhere. Of
tbo work of the age of chivalry proper, tbe chansons dc gestes^ the
Arthurian romances, the early lyi'ics anil dramas, he evidently knew
but little, and chose to subordinate what he did know to his general
theories of the time. Even nmcb later bis praise and blame, though
transparently honest, arc quite haphazard. Unless, therefore, the
reader be gifted with a very rare faculty of applying the " grain of
salt" to what he reads, or unless be be well acquainted with ths
actual facts before coming to Jlicbelet's veraion of them, he will
almost certainly be misled. But despite this grave di-awback
(which attends all picturesque Iiistory) the value of Micbelct merely
as an histeriau is immense. Kot only are his sei>arate tableaux,
tlic wonderful geographical sketch of Fi-ance in the beginning of
tbe book, the sections devoted to the Templars, to Joan of Arc, to
the llenaiasaiico, to the Camisards, almost unequalled, but the in-
spiriting and stimulating effect of bis w-ork is not to bo surjvissed.
If bis reconstruction is often hazardous and conjectui-al, sometimes
definitely and demonstrably mistaken, and nearly always difficult
to adjust entirely to the ascertained facts, it is always possible in
itself, always instinct with genius, and always life-like. There are
no dead bones in Slicbclet ; tlu-y ai-e if anything only too stirring
and lively. These criticisms apply equally to the minor books,
though these are necessarily fuller of the author's somewhat weari-
some propaganda, and less full of brilliantly painted facts. Tbe
great fault of .Michelet as of not a few other modern authors is tbe
compai-ativcly improvised and epbemcr^fl character of too much of
bis work. His immense volume is, much of it, mere brilliant
pamphleteering, much more mere description equally brilliant Cut
equally liable to pass. Nevertheless he is (especially in Frcndi, the
language jiar a:alUna of measured and acadenjic )icrf6ition) so
characteristic and singular a figui-c in his turbid eloquence and
fitful flashing insight that ho is never likely to lose a place, and a
notable one, in literary history.
Almost idl Michelet's works, the exceptions being his translations,
compilations, &c. , are published in uniform size and in about fifty
volumes, partly by Marpon and Flammarion, partly by Calniann
Levy. (G. SA.)
MICHELL, jOH\% an eminent Englisli man of science
of the 18tli century. He received his university education
at Queen's College, Cambridge. His name appears
fourth in tlife Tripos list for 17-18-49 ; and in 1755 he was
moderator in that examination. He was a fellow of his
coUegc'and became successively AVoodwardian professor
of geolog)' (in 17021 and rector of Thornhill in Yorkshire.
He >vas«lected a member of the Royal Society in tho .-(ame
yeai as Henry Cavendish (1700). Ho died in 1793. In
1750 he published at Cambridge a small work of soma
eighty pages, entitled A Treatise of Artijicial Magnets, in
which is eliotm an easy and ejrjyedilurus melhud of luaMnff
them miperior to the Oest natural mies. Besides the descrip-
tion of the method of magnetization which still bears his
name, this work contains a variety of acute and accurate
magnetic observations, and is particularly distinguished by
a lucid exposition of the nature of magnetic induction.
He is now best kuowu as the original inventor of the torsion
balance, wliicli afterwards became so famous in the hands
of its second inventor Coulomb. Midiell described it iu
his proposal of a method for obtaining the mean density
of the earth. He did not live to put his method iato
practice ; but this was done by Henry Cavendish, who
made, by means of Jlichell's ap[)aratus, the celebrated
determination that now goes by the name of Cavendish's
experiment {PhiJ. Trans., 1798).
ilicbeirs other contributions to science are — " Conjectures con-
cerning tbe Cause and Observations ujion tbe rbcjiomena of Earth-
3uakes," Phil. Trai's., 17G0 ; "Observations on the Comet oC
anuary 1760 at Cambi-idge,'' /&., 17C0 ; "A Bcconimendation oT
Hadlcy's Quadrant for Surveying," 10., 1765 ; " ri-oposal of a
Method for measuring Degrees of Longitude upon rar.allels Of tbo
Equatoi"," 76., 17C6 ; "An InquiiT into the Probable Parallax and
llaguitudeof the Fi.xed Stars,' 11., 1767 ; " On the Twinkling of
the Fixed Stars," It/., 1767 ; "On tbe Means of Discovering the
Distance, Magnitude, kc, of the Fixed Stars," lb., 1784.
MICHELOZZI, MicHZLOzzo (1391-U72?), was a
Florentine by birth, the son of a tailor, and in early life a
pupil of Donatello. He was a sculptor of some ability in
marble, bronze, and silver. The statue of the young
Sb John over the door of the Duomo at Florence, opposite
the Baptistery, is by him ; and he also made the beautiful
silver statuette of the Baptist on the altar-frontal of San
Ciovanni. Michelozzi's great friend and jjatron was Cosimo
I. dei Medici, whom he accompanied to Venice in 1433
during his short exile. AMiile at Venice, Michelozzi built
the library of San Giorgio Jlaggiore, and designed other
buildings there. The magnificent Palazzo dei Medici at
Florence, built by Cosimo, was designed by him ; it is one
of the noblest si)ccimens of Italian 15th-century architec-
ture, in which the great taste and skill of the architect has
combined the delicate lightness of the earlier Italian Gothic
with the massive stateliness of the Classical style. With
great engineering skill Michelozzi shored up, and partlj*
rebuilt, the Palazzo Vecchio, then in a ruinous condition,
and added to it many imixjrtant rooms and staircases.
AMien, in 1437, through Cosimo's hberality, the monastery
of San Marco at Florence was handed over to the Dominicans
of Fiesole, Michelozzi was employed to rebuild the domestic
part and remodel the church. For Cosimo I. he designed
numerous other buildings, mostly of great beauty and
importance. Among these were a guest-house at Jerusalem,
for tlie use of Florentine pilgrims, Cosimo's summer villa
at Careggi, and the strongly fortified palace of Cafagiuolo
in Mugello. For Giovanni dei Medici, Cosimo's son, he
built a very large .and magnificent palace at Fiesole. Iu
spite of Vasari's statement that he died at the age of
sixty-eight, he appears to have lived till 1472. He is
buried in tho monastery of San JIarco, Florence. Though
skilled both as a sculptor and engineer, his fame chiefly
rests on his architectural works, which claim for him a
position of very high honour even among the greatest names
of the great 15th-century Florentines.
MICHIGAN, one of the States of the American Union, Plate I^
situated in the region of the great lakes. It lies between
41° 42' and 47° 32' N. lat, and 82° 24' and 90° 31' W.
long., the centre of the State being 670 miles norti of west
from New York, the nearest point on the seaboard. The
area is 58.915 square miles. The State consists of two
238
MICHIGAN
nat'jral divisions, known as tlie Upper and tlio Lower
peninsula. Tho Upper or Northern Peninsula is bounded
on the N., E., and S. by Lakes Siiperior, Huron, and
Michigan, and on the W. by the river St Mary and the
State of Wisconsin. The Lower Peninsula is bounded on
the W., N., and E. by Lakes Michigan, Huron, St Clair,
and Erie, and the St Clair and Detroit rivers, and on the
S. by the States of Ohjo and Indiana. The general contour
of the Lower Peninsula approaches that of a horse-shoe,
with an average width of about 200 miles from east to
-.vest and a lenplit oi about 300 miles from north to south.
l\j. surface gradurlly rises ir. gentle undulations from the
r.'j:rounding iaktb to an elevai ion of about 400 feet above
I cie Huron, no point reacl/ing an altitude of more than
600 feet. The Upper Peninsula is much more rugged in
coutour and surface, at some points reaching an. elevation
of about 1100 feet. The territory was originally covered
with forests, with only here and there a small open prairie.
It dbotrnds in fine inland lakes, with areas varying from
a few acres to several miles. The rivers are not large
enough to be navigable, but they afford ample v/ater-power,
and are particularly valuable for floating down the log-? of
the lumbering districts. The coast-Une of the State is not
le.ss than about 1600 miles in length ; and along the whole
of this distance vessels of 2000 tons mUy , pass without
losing sight of land.
Geological Formation. — The Lower Peninsula~occTtpies
the central part of a great basin, the borders of which
extend to the east as far as London, Ontario, and to the
west as far as Madison, Wisconsin. Within these limits'
the traveller starting in any direction from the centre of
the State encounters successively the outcropping edges
of older and older strata. The whole series has been
iiiened to a nest of wooden dishes ; it embraces not
only the Laurentian and Huronian systems but also
the numerous groups that go to make up the SUufian,
ttie Devonian, the Carboniferous, and the Quaternary
systems. These several formations are covered almost
oiiiversally with a drift of finely comminuted and triturated
rock,,, borne thither by moving glaciers and floating
icebergs, or washed to its present position by currents
of water, while the surface was still submerged. This
loose material varies in thickness, sonietimes extending to
a depth Of 200 or 300 feet. '^Tiile the lower formations
contain almost inexhaustible deposits of copper, iron,
gypsum, and salt, the surface soil is pre-eminently fertile,
uniting aU the mineral constituents necessary for the most
luxuriant growth of plants.'' There are limited areas of
light and somewhat sterile drift soil; but even these
have shown themselves under proper treatment to be
capable of yielding a rich . vegetatioin. For the most
part the drift soil i3 composed of a, mixture of clay
with sand and gravel. It is easily cuiJtivated, is retentive
of moisture, and is sufficiently porous to prevent the injury
of crops by excessive rains. '\
Climate and Natural Products. — The mean temperature
of Lansing, the capital of the State, as determined by
ob.servations extending through eighteen years, is 46°'7I-
Fahr., or about the same as that- of Berlin. During the
summer months the mean temperature is nearly the same as
that of Vienna ; in the winter it is nearly that of Stockholm."
The annual rainfall during the eighteen years previous to
.1382 was about 31 inches. This is very evenly distributed
■i . •oughout the year, though a little more than half the
Avaount falls in the five months from May to October.
Tha eTe»a.ge snowfall in the centre of the State is about 4
f sat, thoii.gh it is seldom that more than 1 2 inches lie on the.
{.Tound r.t any one time. The winter temperature is much
modified by the open water of the aJjaceat lakes The
. BBvere wiuda ar3 commonly from the west and nprtij-west ;
but in sweeping across the open waters of Lake Midugftft
they are so far' softened as to' make the climate much
milder than that found in the same latitude on the western
side of the lake. • This pecuharity is specially favourable to
the growth of fruits. ■ Peaches are grown successfully along
the 45th parallel, and figs thrive in the open air in lat. 42J*.
The modifying influence of the lake winds also gives great
variety to the flora. The predominant woods are oak, maple,
beech, elm, ash, cherry, hickory, walnut, basswood, and pine.
All these grow luxuriantly in the vast forests of the State,
and afford an abundant supply of the best timber. There are
1G5 species of trees and shrubs indigenous to Michigan;
and the entire flora of .the State_makes a list of 1634
species.
Cereals and Fruits.- — The most important cropof Michigan-
is wheat, and the average jntld per acre, as shown by ths
latest census, is greater than that of any other State in the
Union. The acres sown in 1879 were reported as 1,822,749,
and the amount produced as 35,532,543 bushels, i These
figures show that Michigan is fourth in rank of the wheat-
producing States, the number of bushels grown' being
exceeded by the crops of Illinois, Ohio, and Indiana. In
1879 the j-ield in bushels of the other principal cereals in
shovm by the following figures : — Indian com, 32,461,452 j
oats, 18,190,793; barley, 1,204,316; rye, 294,918; buck-
wheat, 413,062; clover seed, 31.3,063; pease, 538,332.
The crop of potatoes in the same year was 8,025,475
bushels, and the hay amounted to 1,051,115 tons. Of
the fruits grown in the State apples are the most important,
and these are believed to be unsurpassed in excellence i»
any country in the world. The sales in 18S0 were
4,834,936 bushels, a considerable qiiantity going to the
markets of Europe. Next in importance is the peach crop,
annually gathered from more than fifty of the counties of
the State. In 1880 the peach orchards were reported .as
covering 12,908 icres, and the fruit sold as amounting to
413,418 bushels. •; The long coast-line of Lake Michigan
affords easy access to market even for the most perishable
fruits. ■ Besides the facilities thus afforded, the railroad*
that now thread^the State, with an aggiegate length in
March 1882 of ^43.'?2,mile.9, afford abundant means of
rapid transportation. As the fruit belt extends from north
to south more than 200 miles, the danger of disastrous
competition in the niarkets is obviated by prolongation of
the season of ripening. At the meeting of the State
Horticultural Society held in 1881 it was reported that
the average value of the peach crop per acre vs-as above
$125. r- The ten volumes of the Transactions of the State
Horticultural Society published since its organisation in
1670 show that the development of fruit culture within
the last decade has been much more rapid than in any
other State.
Lumber. — The timber produce in ^ndiigan is of superior
quality, and the amount is so great that about two-thirda
tif the best lumber^ sold in New York, Philadelphia, and
Boston go out from its mills. The log? are borne along
the lakes, rivers, and small watercourses to the booms of
mills situated at convenient ijoints, where the lumber is
isawed and shipped for the different markets of the world.
Of these manufacturing districts those kjiown as the
Saginaw, the Grand River, and the Muskegon valleys are
the most important. ' The Saginaw receives the waters of
the Tittabawasse, the Cass, the Flint, the Shiaw-assc, the
Bad, the Pine, tTio Chippewa, the Tobacco, and their
numerous tributaries, draining a vast,rcgion that still yields
an undiminished supply of piws. The foresU of the western
parts of the State are easily accessible by the Grand River
and its tributaries, while those still farther iicrtli find a
natural outlet through the numcrdts streams iLit flv:/winto
Lake Michigan. On the iSinks of these watercourses are
MICHIGAN
239
some of the largest and finest mills of the world. In 1854,
when the first effort was made to collect statistics of this
industry, it was found that there were only sixty-one mills
in operation, and that the entire annual product was only
108,000,000 feet. Eighteen years later, in 1872, it was
estimated that the annual product was i)ot less than
2,560,000 feet of oak, 12,700,000 of staves, 300,000,000
lath, 400,000,000 shingles, and 2,500,000,000 of sawed
pine. The number of saw-mills had already reached about
1500, the number of persons employed 20,000, and the
capital represented S35,000,000. In 1881 the manufacture
of pine lumber amounted to 3,919,500,000 feet, the value
of which 'exceeded $60,000,000. The aggregate value of
the forest products of the State was estimated in 1881
to have reached more than §1,000,000,000. Forestry
BuUelin, No. 6, issued December 1, 1881, estimated the
amount of standing white pine of merchantable quality at
35,000,000,000 feet, and the amount of standing hard
wood at 700,000,000 cords. Besides these amounts, the
same authority estimates the amount of hemlock at
7,000,000,000 feet, with 7,000,000 cords of bark, and an
aggregate of 70,000,000 of cedar and tamarack. It is
probable that before many years the hard wood ptoduced
by the State will approach in value the figures representing
the value of the pine now sent to the markets of the world.
It is probable that Michigan for many years to come will
maintain its precedence as a lumber-producing State.
Mhieral Resources. — Of the mineral products of Michigan
the most important is iron. As early as 1842 the report
of the first State geologist, Dr Douglas Houghton, called
attention to the presence of haematite ore, though for a
considerable time after this it was not found in such
ouantitibs as to make it certain that mining could be made
profitable. Before 1860, however, it became known that
iron in the Upper Peninsula not only existed in vast
rjuantities, but also that it was of superior quality. From
that time iron-mines were rapidly developed, until in
1881 they had come to exceed in value, though not in
amount, even the products of Pennsylvania. In 1880
the product was 1,834,712 tons, with a value at the mines
of §6,034,648, as against the yield in Pennsylvania of
2,185,675 tons, with a value of §5,517,079. The product
of Michigan in 1882 was 2,948,307 tons of ore, with a
market value of about $25,600,000. The ilichigan
minerals are of extraordinary richness, — 62'9 per cent,
being the average of the first^dass ores, while the furnace
books often show a much higher yield.
Next in importance to the iron-mines are those of copper.
These are also situated in the Northern Peninsula, in the
mountain range of trappean rocks which crown tlie point
of land extending northwards into Lake Superior. Tliis
secondary peninsula or cape, known as Keweenaw Point,
rises to an average height of about 600 feel, above the lake,
the highest pinnacles reaching nearly double that altitude.
This point contains what are believed to be the richest
copper-mines ever discovered ; the metal is not found as
an ore, but as virgin copper almost chemically pure. It
has only to be separated from its rocky matrix, when it is
ready for the market. The largest of the copiier-mines,
tliat at Calumet, has built up an industry whicli employs
2000 men, and its total product of refined copper in 1S82
was no less than 50,770,719 lb, or one-eighth of the
annual production of copper in the world. In quality the
copper of the Lafie Superior district ia^ such that it com-
mands the highest price at home and abroad. Its tenacity
is remarkable, and therefore it is eagerly sought after for
cartridges by all the great military poweA. In 1882 the
copper-mines paid dividends amounting to $2,900,000, —
maiing an aggregate of $28,248,000 since they were \jp
opened. 't^
Within a few years the salt-works of Michigan have also
come to exceed those of any other State in the Union.
The first well was sunk in 1859-60, but in 1882- the pro-
duction was found to have exceeded that of the famous
works in New York, and to have amounted in that year
to no less than 3,204,921 barrels. The extraordinary
development of this industry is due to several causes. A
careful system of inspection by State authority has kept
its salt unsurpassed in purity. The salt basin is not only
accessible by navigable waters, so as to have the advantage
of cheap transportation, but the welLs are situated in the
great lumber-producing districts, and the manufacture is
thus carried on at very small expense, in connexion
with the saw-mills. The power is furnished by the same
engines, the exhausted steam is used for the evaporation
of brine during the day, and during the night evapora-
tion is still carried on by means of refuse wood and saw-
dust, while the staves for barrels are made from rejected
timber. By this system the best quality of salt is obtained
at a minimum expense. The chief reservoir of salt is the.
series of sandstones and shales constituting the Waverly
group. This salt-producing rock covers no less than about
8000 square miles, and it is safe to presume that the supply
is inexhaustible. The average depth of the w4Us is about
800 feet, but in some localities wells sunk to nearly 2000
feet have been remunerative. Important salt-works have
recently been developed in the western part of the State.
There are also certain other minerals of considerable
importance. Deposits of gypsum, easily accessible, prac-
tically inexhaustible in quantity, and superior in quality,
are found in several localities both in the eastern and in
the western parts of the Lower Peninsula. In the outskirts
of Grand Rapids the deposit crops out at the surface, and at
an average depth of from 40 to 70 feet extends over an
area of 1 0 or 12 square miles. The rock is easily quarried,
and is either ground for use as a fertilizer or calcined into
plaster of Paris. The deposits of coal are supposed , to
cover about 8000 square miles, but as yet the product
at any one point has not been very considerable. In
quality the coal is highly bituminous, and is not sulficiently
pure to be useful for smelting or for the manufacture of
gas. For these reasons the stock of coal in the State is
practically untouched. If future explorations and experi-
ments should make these 'ieposits available, a new era in
the manufacture of iron will be the result. At present
the coal for smelting the Lake Superior ores is brought
chiefly from Ohio and Pennsylvania. Quarries of lime-
stone and of sandstone have been opened in various parts
of the State. ^ The brown stone of the Upper Peninsula is
of excellent quality, and is cajiable of receiving a high
finish. The supply is inexhaustible, and the accessibility
of the quarries by water gives promise of a thriving
industry. The grindstones taken from the Huron county
quarries are of superior quality, and the slates found in
unlimited quantities on the shores of the Huron Bay are
unsurpassed in point of durability and colour. Clays and
sands of commercial value are found in great abundance.
Though the manufacture of glass is yet in its infancy,
sands in large quantities have been discovered in Monroe
county suitable for the manufacture of plate glass of excel-
lent quality. jjBrick and tile clays are found in all parts of
the State. Though native silver has been found in small
quantities in the Upper Peninsula, the systematic mining
of this metal has not yet been carried on with successful
results. The Report of the commissioner of mineral
statistics for 1882 shows that, except as to coal, -Alicliigaii
is the foremost of all the States in mineral w^th.
Fisheries. — Tlie gooRraiiliical position of Jlicliigan fcplains tV.i;
ct that its frcsh-w.Ttcr fisheries are the most productive ia OuO
ui'ed States. Tlie most iiuuoitout vai'ii.ties uf &sh are lakc-twut.
240
MICHIGAN
sturgeon, bass, pictorC), Lornng. 6rook-tTont. prnylinj;, and wliitc-
fish. Ocncnil laws for the protection of fish have been passed ; ami
a fish commission haa been maintiiDcd for some years for the
purpose of propagating the best varieties and plunting them in
wfttei-3 ailapteii to their naturnl development. Up to tlio close of
1880 tJie commissioners had planted about 80,000,000 young white-
!ish, 1,000,000 silver eels, 1,000,000 lake-trout, 2,000,000 salmon,
and 500,000 brook-trout, besides smaller numbers of shad, grayling,
pike, and bass. Excellent results have followed, especially in the
multiplication of white-fish, salmon, and eels. In 1879 the tntul
"lake" was 24,013,100 lb, of which 12,902,250 lb were white-lish,
tho most valuable lake-fish known to epicures and to commerce.
During winter large quantities preserved by freezing ore taken to
Eastern markets, where they are readily sold at a high price.
Ethicationnl Institutions. — As early as 1785 the law of congiess
which provided for the sale of lands north of the Ohio river reserved
for the support of public schools "section 16" of each township.
This fundamental law devoted to educational purposes one-thirty-
sixth of all the lands of that vast domain known aa the north-
western territor}'. The "ordinance of 1/87," by which this
teiTitory was or^'anized, further provided that "schools and the
means of education shall for ever be encouraged," In 1S26 this
eoDgressional action was supplemented by a grant to Michigan of
two townships of land for the founding and support of a university.
When llichigan became a State in 1837, its educational policy took
definite form. The constitution provided, not only that the grant
of "section 16" should be devoted exclusively to the supjwrt of
schools of the primary grad^, but also that the State and not each
township should be the custodian of the lands so appropriated.
Tlie constitution expressly provided that the proceeds from the
said of "school lands'' should be held by the State as a perpetual
fund, the interest of which should be annually applied to the sup-
port of primary schools. The lands devoted to school purposes in
Michigan under these provisions amounted to 1,077,209 acres, of
which, in September 1881, 675,000 acres had been sold. On the
sum realized by these sales, $3,095,679, the State pays interest at
7 per cent., and the resulting income, amounting to $216,645, is
annually distributed to the scliools. This source is supplemented
from local taxes, so that in 1881 the total sum realized from a'l
sources for the primary schools was $3,644,778.
Th6 schools organized under State law arc known as graded and
nngradeil. In the small districts where the schools are under the
charge of but one or two teachers, grading is impracticable. Of
ungraded districts there were in 1881 6120, attended by 219,570
children, while the graded schools were 404 in number, with au
attendance of 152,043. The school census includes all children
between the agesof five and twenty, amounting in 1881 to 518,317, of
whom there was an average attendance of 391,401. To all children
of school age the public schools arc free, though a fee may be re-
quired for advanced studies in the high schools. The immediate
administration of the schools is entnisted to school officers elected
annually by the tax-payers of the individual districts. The State
constitution requires that a free school shall be in session at least
three months of every year in each district. In districts of more
than 30 and less than SOO children, the law rcouires at least five
months of school ; while in districts of more than SOO children,
the session must be not less than nine months in length. In the
graded schools the division is into primary schools, grammar schools,
and hi^h schools, each of these divisions retaining the scholar
ordinarily four years. At the end of the course the student is ready
for the university, to which, under certain restrictions provided by
tho luiiversity itself, he is admitted on diploma from the high
Hchool. The uAiversity of Michigan, situated at Ann Arbor, was
first opened for insti-uction in 1841. It now (1883) consists of the
department of literature, science, and the arts, the department
of medicine, tht department of law, the college of homoeopathic
medicine, the school of pharmacy, the college of dental surgery,
and tho school of politicnl science. Connected with the medical
departments are the State hospitals. In 1881-82 there were 86
officers of instruction and 1534 students. The total income for the
year 1879-80 from Federal grant, State grants, and foes \va3
$231,339. The general control of the university is placed in the
hands of eight regents elected by popular sufTrage at tho biennial
spring elei'tious, two regents being chosen at each election. Tho
normal school, situated at Ypsilanti, and generously supported by
tho State, may be said to complete the school sjstem.
Charitable and Jxc/ormatory InstitiUions. — A school for the dcnf,
dumb, and blind, instituted under an Act pa.ssed in 1848, is situated
at Flint, about 60 miles north-west of Detroit ; in February 1882 it
had 249 pupils. In 1879 a distinct school for the training of tho
blind was established nt Lansing. Tho " State public school for
dependent and neglected children" is devoted to the systematic
education of such cnildrcn as otherwise would have to bo maintained
in the county poorhouscs. The pupils are divided into "families"
of about thirty cacli, and arc cared for in separate cottages, each
cottii'^c being under the charge of a "onttiigc malinger." Thn
school receives dependent children of sound health, and free from
contagious disease ; and it is made the aory of tho officers having
charge of tho poor to send all such cliildr^n between the ageh (.!
three aiid twelve to it. Tliis institution, the pioneer of ita kind,
and one of the most useful of charitable schools, is situated at Cold-
water, 132 miloa south-west of Detroit In February 1882 there
were 320 children and 21 officers and teachers. The "Ileform
School" at Lansing is desigutd to ret^Iaini juvenile ofifendcrs who
have been convicted of some olfence. A farm of 224 acres connected
with the school is, in considerabio part, tilled by tho boys. Tho
number of inmates in February of 1882 was 325. A similar school
at Adrian has recently betn iiislituttd for girls. There are State
asylums for the insane at Kalamazoo (715 patients) and Pontiac
(499 patients). The legislature of 1S81 provided for tho establish-
nient of an additional asylum in one of tho northern counties of the
Lower Peninsula.
Populaiioyt. — ln 1837 tho State had 174,647 inhabitants. The
numbers according to the different census returns from 1840 are
given in the foUou-ing table ; —
Ceiisoa,
TolaJ.
Malts.
Fcmalca
Densliy per 1
S<iuure Mllr. |
1840
1850
1S60
1870
IS80
!I2,2C7
897,CM
749,113
1,164.050
l,63(i,U37
113.7SS
603.807
304, CM
617.745
bCi,67S
98.479
167.757
3&4.419
774,240
3-T7
7-07
1!U
SOOl
17 80
At the last census 388,508 of the inhabitants were of foreign birtli,
97,346 being natives of the UDiteJ Kingduiu, 89,086 Germans, and
16,445 Scandinavians. In point of population the State, which
was twenty-third in 1840, now stands ninth in the Union.
The following are the principal cities iu the State, with popu-
lation at the censmof 1880:— Detroit, 116,340; Grand Rapids Citv,
32,016 ; Bay City, 20,693 ; East Saginaw City, 19,016 ; Jackson
City, 16,105; Muskegon City, 11,262 ; SaginawCity, 10,525 ; Port
Huron, 8383; Flint City, 8410; Lansing (the State capiial),
8319 ; Ann Arbor, 8061 ; Adrian City, 7849; Battle Creek, 7063;
Manistee, 6930; West Bay City, 6397; Alpena City, 6153-
Ishpcmiug, 6039.
History and Government. — The State of Michigan is part of the
territory that was first settled by the French, and until the fall of
Canada into the hands of the British after the middle of the ISth
century was under the government of New France. The territory
was explored by Jesuit missionaries in tho 17th century ; but,
although it was known at an early period that the lands were
of exceptional excellence, very little progress was made in develop-
ing the resources of the territory untu after tho completion of
the first half-century of the American Union. Tho surveyors
employed by tho general government to inspect tho lauds and
report as to their titness for yeltlement by the soldiers of the war
of 1812 appear to have derived their impressions almost exclusively
from the low lands in the south-eastern comer of the territory. The
report, accordingly, was not favourable ; and consequently the tide
of immigration that had already begun to set in llovved steadily
past Jli-higan into the territories fartlier west. It w.is largely for
this reason that tho early development of Indiana, lllinoi.s, low.i,
and Wisconsin was somewhat more rapid than that of ilichigan.
But gradually the false impressions concerning the soil and climate
were dispelled ; and within tho past few vears the iucrease of the
population and the growth of wealth liavc been very rapid.
In 1851 the valuation of the State for purposes of taxation (which
excludes much v.-iluable jiroperty) was 830,976,270; in 1861,
8172,055,808; in 1871, $630,000,000; at 1881, $810,000,000.
Tho State constitution, adopted in 1837 at thctimeof admission
to tho Union, has boon modified in some minor particnloi-s ; but Id
most respects it remains unchanged. The governor is elected for
two years, with no restriction as to ro-elccti»n. Tho Icgislnturo
meets biennially in the first week of January, and usually continues
in session till Jlny. The supremo court consists of four judges
chosen by popular vote for terms of eight years, ono being elected
every second year. Judges have been so frequently rc-olecled that
the office may be said to be practically a permanent one, with t
provision for termination in case of need. The Slate is divided into
twenty-two judicial districts in each of which a circuit court sits for
tho trial of causes of original jurisdiction, and of causes appealed
from tho justice courts. The judges of the circuit courts are also
elected by popular sulTrage. On political questions voting is open
to all naturalized citizens of the male sex inoro than twenty-one
years of age unless prevented by some natural disqualification. At
school ineetinps tho right of suffrage is extended so as to include
tax-payers of either seit.
/(iir»ori7in.— Frcilcrick Vcflcf.Ulrhtfan and III Rntmretl, compWti nniljc
anthorily of the Slale, Sd eel.- Delroli, 19SJ; ll"oH(»»'i AHat <■/ Utckigat,
vitti an Aeeount of the Topograptiv^ Climalf. and Getfiogg of tht Slate, bjr .\lcx.
Wlnchcll LL.D. : Jamcl V. CaniplKll, OulltneM of the Pclllleal HUlor, «r
Uiehdian: Rrporit tf tht Seerelarg of the Slate Pomolofleat SciMt of tlich<}an
from li71 10 1S80 ; Bepixt of the ioinmiiiUntri^ education for USO: Forlfffit.
1
M I C — M I C
241
Annual Rrpcrl nf llf SipninUndtnlof PMU hitratlion o/lht Stale c/ Uichioan
(or the tear ISal; Rporls of lUe Ocdloyi'al Suireii (■/ Iht Slalt «/ Micliigaa.
1869-80 4 vols. : Sf'Ciat Report 0/ Coinmistioiter of iliutrat Slatistirt, March
1883 ; Fcreili) Oulleliat (or 1881. (C K. A.)
MICHIGAN, Lake. See St Lawrence.
MICHIGAN CITY, a town of the United States, in
Laporte county, Indiana, on the south-east shore of Lake
Michigan, 40 miles east-sonth-east of Chicago. As a
lake-port and a junction for several railroads, it is a
place of considerable prosperity. It is the largest lumber-
market in the State, and one of the largest in the. west,
and has numerous manufacturing establishments. The
northern State prison (with 577 convicts at the close of
1880) is one of the principal buildings. The jiopulation
increased from 3985 in 1870 to over 10,000 in 1883.
MICHMASH (E'»??P, D??P), the scene of one of the
most striking episodes in Old Testament history (1 Sam.
liv., comp. vol. xii. p. 403), was a place in Benjamin,
about 9 Roman miles north of Jerusalem (Onom., ed. Lag.,
p. 280). Though it did not rank as a city (Josh, xviii.
21 sq.), Michraash was recolonized after the exile (Xeh. xi.
31), and, favoured by the possession of excellent wheat-
land (3fishna, Men. \iii. 1), was still a very large village
(Max^a'j) in the time of Eusebius. The modern ilakhmiis
is quite a small place.
The liistorical interest of Jlichmabh is connected with the
*tnit>'gical iiii]>artinec of the position, coninianiling tlic uoith siilc
of the Pass of Micliniash, which uiaJc it the licadfjxiartcrs of the
Philistines and tlie centre of their foi-ajs in tlicir attcnijit to quell
the first risinf; under Saul, as it was also at a later date the licad-
Juarters of Jonathan tlic HiTsmonwri. (1 Mac. ix. 73). From
erusalein to Blount Epliraim there -re two main routes. The pre-
sent caravan road keei'S the Iii;^h jijround to the west near the water-
shed, and avoids the Pass ot Miehmash altogether. But anotlier
roate, the in)portanee of which in antiquity may be judged of from
Isa. X. 28 52- , led souttiwards from Ai over an undulating plateau to
Miehmash. Thus far the road is easy, but at Miehmash it descends
into a very steep and rough valley, wliieli has to be crossed before
reasceuding to Geba.' At the bottom of the valley is the Pass of
Uichinash, a noble gorge with precipitous craggy sides. On the
north the crag is crowned by a sort of plateau sloping backwards
into ft round-topped hill. . This little plateau, about a mile east of
the present village of Makhmas, seems to have been the post of
the Philistines, lying close to the centre of the insurrection, yet
possessing unusually good communication with their establishments
on Mount Epliraim by way cf Ai and Uctiiel, and at tlie same time
commanding the routes leading domi to tha Jordan frotn Ai and
Irom Miehuiasli itself.
MICKIEWICZ, Ad.\m (1798-1855), Poli.-^h poet, was
born iii 1798, near Nowogrodek, in the present government
of Minsk, where his father, who belonged to the schlachta
or lesser nobility, had a small pro|ierty. The poet was
educated at the university of Vilna ; but, becoming
involved in some political troubles there, he was forced
to terminate his studies abruptly, and was ordered to live
for a time in Russia. He had already published two small
volumes of miscellaneous poetry at Vilna, which had been
favourably received by the Slavonic jiublic, and on his
arrival at St Petersburg he found himself admitted to the
leading literary circles, where he was a great favourite both
from his agreeable manners and his extraordinary talent
of improvisation. In 1825 he visited the Crimea, which
inspired a collection of sonnets in which we may admire
both the elegance of the rhythtn ind the rich Oriental
colouring. The most beautiful are Tlu Sturm, Bukchi-
ierai, and Graee of the Coioitess Potoda.
In 1828 appeared his Kunrnd Wallairoa, a narrative
poem describing the. battles of knights of the Teutonic
order with the heathen Lithuanians. Here, under a thin
Teil, Mickiewicz represented the sanguinary passages of
arms and burning hatred which had characterized the long
feuds of the Russians and Poles. The objects of the poem,
although evident to many, escaped the Russian censors,
* A Isa. X. 28 describes the invader as leaving .his heavy baggage
.at Miehmash before pushing on through the pass.-
16— U ,
and it was suSered to appear, although the very motto,
taken from Machiavelli, was significant : " Dovete adunque
sapere come sono duo generazioni da combattere . . .
bisogna essere volpe e leone." After a five years' exile in
Russia the poet obtained leave to- travel ; he had secretly
made up his mind never to return to that country or Poland
so long as it remained under the government of the
Muscovites. Wending his way to Weimar, he there made
the acquaintance of Goethe, who received him cordially,
and, jiursuing his journey through Germany, he entered
Italy by the Spliigcn, visited Milan, Venice, and Florence,
and finally took up his abode at Rome. There he wrote
the third part of his poem Ddadij, the subject of which is
the religious commemoration of their ancestors practised
among Slavonic nations, and Pan Tadeusz, his longest
poem, by many considered his masterpiece. A graphic
picture is drawn of Lithuania on the eve of Napoleon's
expedition to Russia in 1812. In 1832 Mickiewicz left
Rome for Paris, where his life was for some time spent
in poverty and unhappiness. He had married a Polish
lady, Selina Szymanowska, who became insane. In 1840
he was appointed to the newly founded chair of Slavonic
languages and literature in the Collige de France, a post
which he was especially qualified to fill, as he was now
the chief representative of Slavonic literature, Poushkin
having died in 1837. He was, however, only destined to
hold it for a little more than three years, his last lecture
having been given on the 28th of May 1844. His mind
had become more and more disordered under the influence
of religious mysticism. His lectures became a medley of
religion and politics, and thus brought him under the censure
of the Government. A selection of them has been published
in four volumes. They contain some good sound criticism,
but the philological part is very defective, for Mickiewicz
was no scholar, and he is obviously only well acquainted
with two of the literatures, viz., Polish and Russian, the
latter only till the year 1830. A very sad picture of the
declining days of ilickiewicz is given in the memoirs of
Herzen. At a comparatively early period the unfortunate
poet exhibited all the signs of premature old age ; poverty,
despair, and domestic affliction had wrought their work
upon him. In 1849 he founded a French newspaper,
La Tribune des Pevples, but it only existed a year. The
restoration of the French empire seemed to kindle his
hopes afresh ; his last composition is said to have been a
Latin ode in honour of Napoleon III. On the outbreak
of the Crimean War he was sent to Constantincple to assist
in raising a regiment of Poles to take service against the
Russians. He died suddenly there in 1855, and his body
was removed to France and buried at Montmorency.
Mickiewicz is held to have been the greatest Slavonic poet, with
the exception of Poushkin. Unfortunately iu other parts of Europe
he is but little known; he writes in a very difficult language, and
one wliieh it is not the fashion to learn. There were both patho.s
aiul irony iu the expression used by a Polish lady to a foreigner,
" Kous avons notrc .Miekienicz k nous." He is oue of the best pro-
ducts of the so-called romantic school. The Poles had long
groaned under the yoke of the classicists, and the country was full
of legends and picturesque stories which only awaited the coming
poet to put them into shape. Hence the great popularity among
liis countrymen of his ballads, each of them being connected with
some national tradition. Besides KonraJ Walknrod and Fan
TaJcusz, attention m.iy be called to the poem dnzi/ua, which
describes the adventures of a Lithuanian ehifftainess against the
Teutonic knights. It is said by Ostrowski to have inspired the
brave Emilia Plater, who was the heroine of the rebellion of 1830,
and after having fought in the ranks of the insurgents, found a
grave in the forests of Lithuania. A fine vigorous Oriental pieeeis
Fanjs. Very good too are the odes to Youth and to the his-
torian Lelewel ; the former did much to stimulate the eflorts of the
Poles to shake off their Russian conquerors. It is euougK to say
of Miekiewiez that he has obtained the proud position of the repre-
sentative jioet of liis country ; her customs, her superstitions, her
history, her struggles are reflected in his works. _,^
242
M I C — M I C
illCKLE, WiLUAM Julius' (1734-1788), son of the
minister of Langholm, Dumfriesshire, holds a respectable
place among the imitative minor potts of the 18th century.
He wrote a poem on Knowledge — carefully versified,
pointing a moral on the vanity of intellectual pride —
af the age of eighteen, entered into business as a brewer
at his father's request and against hia own inclinations,
soon became bankrupt, went to London on outlook for
work as a man of letters, solicited patronage in vaiil,
earned a living hardly by writing for magazines, made
some impression in 1765 by "a poem in the manner of
Spenser " called the Concubine (afterwards Syr Martyn),
was appointed corrector to the Clarendon Press, and finally
took a place among the leading poets of that very barren
time by a translation of the Lusiad of Camoens into heroic
couplet^ (specimen published 1771, whole work 1775).
So great was the repute of the work that when Mickle —
appointed secretary to Commodore Johnstone — visited
Lisbon in 1779 the king of Portugal gave him a public
reception. As a translator of Camoens Mickle has been
superseded, but he aimed, not at close rendering of the
original, but at making a poem which should be worthy of
a permanent place in English literature. This ambition
he waa not capable of fulfilling^ though he had great
fluency and vigour. It may be doubted whether the
fashionable forms which he imitated were the best suited
to hia natural gifts. He shows delight in lively action, a
sense of dramatic effect, and, in the Concubine, the sub-
stance of which might have been conceived by Crabbe,
considerable fulness of detail in coarse realistic painting.
Certainly, if the Scottish poem There 's nae luck aboot the
hoose was Mickle's, he mistook hia medium. Scott read
and admired Mickle's poems in his youth, and, besides
founding Kenilworth on the ballad of Cumnor Hall, waa a
good deal influenced by liim in style. Mickle's prose is
lively and vigorous.
MICROMETER, an ■ instrument . generauy applied to
telescopes and microscopes for measuring small angular
distances with the former or the dimensions of small
objects with the latter.
Before the invention of the telescope the accuracy of
astronomical observations was necessarily limited by the
angle that could be distinguished by the naked eye. • The
angle between two objects, such as stars or the opposite
timbs of the sun, was measured by directing an arm
furnished with fine " sights " (in thi sense of the " sights "
of a rifle) first upon one of the objects and then upon the
other, or by employing an instrument having two arms
each furnished with a pair of sights, and directing one
pair of sights upon one object and the second pair upon
the other. The angle through which the arm was moved,
or, in the latter case, the angle between the two arms, was
read off upon a finely graduated arc. With such means no
very high accuracy was possible. Archimedes concluded
from his measurements that the sun's diameter was greater
than 27' and less than 32' ; and even Tycho Brahe was so
misled by his measures of the apparent diameters of the
sun and moon as to conclude that a total eclipse of the sun
was impo3.sible.^ Maestlin in 1579 determined the relative
positions of eleven stars in the Pleiades (Hisloria Coele^is
Litcii Baretti, Augsburg, 1666), and Winnecke has shown
(Monthly Notices R. A. S., vol. jcxxix. p. 146) that the
probable error of these measures amounted to about
±2'."
: .-I
* Grant, History o/ Physical Astronomy, p. 449.
• This is an astonishing accuracy when the difliculty of the olijecta
is considered. Few persons can see with the nuked eye — much less
meacjure— more than six stars of the Plci.ides, although all the siavs
measured by Maestlin have been seen with the naked eye by a few
indivldaals of exceptional powen pf eye*8ight.
The invention of the telescope at once extended the
possibilities of accuracy in astronomical measurements.
The planets were .shown to have visible disks, and to be
attended by satellites whose distance and position angle
relative to the planet it was desirable to measure. It
became, in fact, essential to invent a " micrometer " for
measuring the small angles which were thus for the first
time rendered sensible. There is now no doubt that
William Oascoigne, a young gentleman of Yorkshire, was.
the first inventor of the micrometer. Crabtree, a friend of
his, taking a j^^omey to Yorkshire in 1639 to see Gascoigne,
writes thus to his friend Horrocks. " The fii'st thing Mr
Gascoigne showed me was a large telescope amplified and
adorned with inventions of his own, whereby he can take
the diameters of the sun and moon, or any small angle in
the heavens or upon the earth, most exactly through the
glass, to a second." The micrometer so mentioned fell
into the possession of Mr Richard Townley of Lancashire,
who exhibited it at the meeting of the Royal Society held
on the 25th July 1667.
The principle of Gascoigne's rnicrometer is that two Oas-
pointers, having parallel edges at right angles to the "^ig"'
measuring screw, are moved in opposite directions sym- """''
metrically vrith and at right angles to the axis of the
telescope. The micrometer is at zero wheft the two edges
are brought exactly together. The edges are then separated
till they are tangent to the opposite limbs of the disk of
the planet to be measmed, or till they respectively bisect
two stars, the angle between which is to be determined.
The symmetrical separation of the edges is produced and
measured by a single screw ; the fractions of a revolution
of the screw are obtained by an index attached to one end
of the screw, reading on a dial divided into 100 equal
parts. The whole arrangement is elegant and ingenious.
A steel cylinder (about the thickness of a goose-quill),
which forms the micrometer screw, has two threads cut
upon it, one-half being cut with a thread double the pitch
of the other. This screw is mounted on an oblong box
which carries one of the measuring edges ; the other edge
is moved by the coarser part of the screw relatively to the
edge attached to the box, whilst the box itself is moved
relatively to the axis of the telescope by the finer screw.
This produces an opening and closing of the edges
symmetrically with respect to the telescope axis. Flam-
steed, in the first volume of the Historia Coelestis, has
inserted a series of measurements made by Gascoigne
extending from 1638 to 1643. These include the mutual
distances of some of the stars in the Pleiades, a few observa-'
tions of the apparent diameter of the sun, others of the
distance of the moon from neighbouring stars, and a great
number of measurements of the diameter of the moon. Dr
Bevis (Phil. Trans., 1773, p. 190) also gives results of
measurements by Gascoigne of the diameters of the moon,'
Jupiter, Mars, and Venus with his micrometer.
Delambre gives^ the following comparison between the re-"
suits of Gascoigne's measurements of the sun's semi-diameter
and the computed results from modern determinations : — '
OctoJ)er 25 (O.n.j ...
31. „■ ...
December 2 ,, ...
Gascoigne, from his observation.s, deduces the greatest
variation of the apparent diameter of the sun to be 35" ;j
according to the Connaissance des Temps it amounts to
32"'3.' These results prove the enormous advance attained
in accuracy by Gascoigne, and his indisputable title to tha
credit of inventing the micrometer.
Huygens, in his Systema Saluriiium (1669),"deicribe8
a micrometer with which he determined the apparent
', Delambre, Bist. Ast. Modeme, vol. li. p. 690. >"'
Gascoigne.
Conn. d. Tempi.
16' U"orlO"
16' 10"-0
16' 11"
16' U"-4
16' 24" ,
16' 16"-8 ,
MICROMETER
243
diameters of the principal planets. He inserted a slip
of metal, of variable breadth, at the focus of the tele-
scope, and observed at what part it exactly covered the
object under examination ; knowing the focal length of the
telescope and the width of the slip at the point observed,
he thence deduced the apparent angular breadth of the
object. The Marquis Malvasia in his Ephemeridet (Bologna,
1662) describes a micrometer of his own invention. At
the focus of his telescope he placed fine silver wires at right
angles to each other, which, by their intersection, formed
a network of small squares. The mutual distances
of the intersecting wires h« determined by counting, with
the aid of a pendulum clock, the number of seconds
required by an equatorial star to pass from web to web,
while the telescope was adjusted so that the star ran parallel
to the wires at right angles to those under investigation.'
In the Phil. Tram., 1667, No. 21, p. 373, Auzout gives
the results of some measures of the diameter of the sun
and moon made by himself, and this communication led to
the letters of Mr Townley and Dr Bevis above referred to.
The micrometer of Auzout and Picard was provided vAth
silk fibres or silver wires instead of the edges of Gascoigne,
but one of the silk fibres remained fixed while the other
was moved by a screw. It is beyond doubt that Huygens
independently discovered that an object placed in the
common focus of the two lenses of a Kepler telescope
appears as distinct and well-defined as the image of a
distant body ; and the micrometers of Malvasia, Auzout,
and Picard are the natural developments of this discovery.
Gascoigne was killed at the battle of Marston Moor on
the 2d July 1644, in the twenty-fourth year of his age, and
his untimely death was doubtless the cause that delayed
the publication of a discovery which anticipated, by twenty
years, the combined work of Huygens, Malvaison, Auzout,
and Picard in the same direction.
^pitt As the powers of the telescope were gradually developed,
mtx. it was found that the finest Mirs or filaments of silk, or
the thinnest silver wires that could be drawn, were much
too thick for the refined purposes of the astronomer, as
they entirely obliterated the image of a star in the more
powerful telescopes. To obviate this difiSculty Professor
Felice Fontana of Florence (Saggio del realgabiiuUo difisica
t di stoi-ia naturale, 1755) first proposed the use of spider
webs in micrometers,^ but it was not till the attention of
Troughton had been directed to the subject by Rittenhouse
that the idea was carried into practice.' In 1813 Wollaston
proposed fine platinum wires, prepared by siirrounding a
platinum wire with a cylinder of silver, and drawing out
the cylinder with its platinum axis into a fine wire.* The
surrounding silver was then dissolved by nitric acid, and
a platinum wire of extreme fineness remained. But
experience soon proved the superiority of the spider web ;
its perfection of shape, its lightness and elasticity, have
lied to its universal adoption.
Beyond the introduction of the spider line it is unneces-
isary to mention the various steps by which the Gascoigne
'micrometer assumed the modern forms now in use, or to
describe in detail the suggestions of Hooke,* Wren,
Smeaton, Cassini, Bradley, Maskelyne, Herschel, Arago)
* Mini. Acad, tits Science?, 1717, p. 78 sq.
' lu 1782 (PhU. Trans., vol. luii. p. 163) Sir W. Herschel
writes : — " I hive in vain attempteJ to fiuit lines sufficiently thin to
eitenil them across the centres of the stars, so th.it their thickness
might b« neglected." It is a matter of regret tliat Fontaua's sugges-
ition was unknown to him.
' Quekett in his Treatise mi the Microscope ascribes to Ramsden the
J)ractical introduction of the spider weh in micrometers. The evidence
^appears to be in favour of Troughton.
* mi. Trans., 1813, pp. 114-118.
«> • Dr Hook« made the important improvement on Gascoigne's
iaicrometer of substituting parallel liairs for the parallel edges of its
original construction (Hooke's Posihuiiioiis Works, p. 497).
Pearson, Bessel, Struve, Dawes, ic, or the successive
productions of the great artjpts Ramsden, Troughton,
Fraunhofer, Ertel, Simms, Cooks, Grubb, Clarke, and
Kepsold. It will be sufficient to describe those forms with
which the most important work has been done, or which
have survived the tests of time and experience.
Before astronomical telescopes were mounted parallactically, the Position*
measurement of position angles w.ia seldom attempted. Indeed, angles,
in those days, the diSiculttes attached to such measures, and to the
measurement of distances with the filar micrometer, were exceed-
ingly great, and must have taxed to the utmost the skill and patience
of the observer. For, on account of the diurnal motion, the direc-
tion of the axis of the telescope when directed to a star is always
changing, so tlmt, to follow a star with an altazimnth mountine,
the observer requires to move continuously the two handles which
give slow motion in altitude and azimuth. -■
Sir William Herschel was the first astronomer who measured HerschelV
position angles ; the instrument he employed is described in Fhil. histru-
Trans., 1781, voL Ixxi. p. 500. It was used by him in his earliest nient. '
observations of double stars (1779-83); but, even in his matchless
hands, the measurements were comparatively crnde, because of the
difficulties he had to encounter from the want of a parallactic mount-
ing. In the case o£ close double stars he estimated the distance in
terms of the disk of the components. For the measurement of wider
stars he invented his lamp-micrometer, in which the components
of a double star observed with the right eye were made to coincide
with two lucid points placed 10 feet from the left eye. The distance
of the lucid points was the tangent of the magnified angles sub-
tended by the stars to a radius of 10 feet. This angle, therefore,
divided by the magnifying power of the telescope gives the real
angular distance of the centres of a double star. With a power oj
460 the scale was a quarter of an inch for every second.
The Modem Filar Miaometer.
When equatorial mountings for telescopes became more general,
no filar micrometer was considered complete which was not fitted
with a position circle.* The use of the spider line or filar
micrometer became universal ; the methods of illumination were
improved ; and micrometers with screws of previously unheard-of
fineness and accuracy were produced. These facilities, coupled
with the wide and fascinating field of research opened up by Sir
William Herschel's discovery of the binary character of double stats,,
gave an impulse to micrometric research which has continued
unabated to the present time. A still further facility was given to
the use of the filar micrometer by the introduction of clock-
work, which caused the telesco^ie automatically to follow the diurnal
motion of a star, and left the observer's hands entirely at liberty.' —
The modern filar micrometer has now assumed forms of five types. Classiflca-
Ti/pe A. — Micrometers in which there are two webs, each mov- tion of
able by a fine screw with a divided head. This is the usual English micro-
form of filar micrometer. meters.
Tyiie B. — Micrometers in which one web is movable by means '
of a fine screw with a divided li«ad, and the other by a screw
without a divided head. The latter screw, in ordinary use, is only
employed to change the coincidence-reading of the two webs, for
eliminating the errors of the micrometer screw. This is the ordi-
nary German form of micrometer as originally made by Fraunhofer
and since by Merz, and employed by the Struves and other principal
Continental astronomers down to the present day.
Type C. — A similar form of micrometer to B, except that the
coincidence-point cannot be changed, — there being no second screw
to alter the position of the fixed web.
Type D. — A micrometer somewhat similar in general construction
to form B, except that, in addition to means of changing the zero
point, there is a screw head by which a fine movement can be given
to the whole micrometer box, in the direction of the axis of the
micrometer screw. This is the modern form of micrometer as con-
structed by Repsold.
Type E. —Micrometers fitted with two eye-pieces for measuring
angles larger than the field of view of au ordinary eye-piece.
The micrometer of type A is due to Troughton ; it is represented Trough-
in figs. 1, 2, 3. Fig. 1 is a horizontal section in the direction of ton's ftlir,
the axis of the telescope. The eye-piece nb consists of two piano- micro-
convex lenses n, b, of nearly the same focal length, and with the two meter.
• Herschel and South (Phil. Trans., 1824, part iii. p. 10) claim
that the micrometer by Troughton, fitted to their 5feet equatorial
telescope, is the first position micrometer constructed capable of
measuring position angles to 1' of arc.
' So far as we can ascertain, the first telescope of large size driven
by clockwork was the 9-inch equatorial made for Stmve at Dorpat by<
Fraunhofer; it was completed in 1825. The original idea appears
to be due to Passemcnt {Mem. Acad., Paris, 1746). In 1757 he pre-
sented a telescope to the king, so accurately driven by clockwork that
it would follow a star all night long. ■
2-W
M l.aK,.0 ME T E R
convex SI Jcs rSc!ii">«n ocncr. ,', They are placed at a distance apart
less than the focal length of a, so that the wives of the micrometer,
which must be ilistinctly seen, are bcyouu !i.' The eyc-picce slides
into the tube c,l, which screws into the brass ring c/, through
two openings in which tlie oblong frame, containing tl>e micrometer
slides, passes. • Tlicse slides are shown in fig. 2, and consist of
brass forks k and I, into which the ends of the screws o and p are
rigidly fitted. Tlie slides are accurately fitted so as to have no
sensible Literal shake, but yet so as to move easily in the direction
of the greatest length of the micrometer bo.';. Jtotiou is communi-
cated to the folks by female screws tapped in the heads 711 aud n
[types of riULE
acting on tlic sci'ews 0 and p rcsiwctively." Two pins /}, r, with
spiral springs coiled ronnd them, pass loosely through holes in the
forks i-, ;, and keep the bearing's of the heads m and « firmly
pressed against the ends of the micrometer box. Tlius the smallest
rotation of eitlier head communicates to the corresponding slido mo-
tion, which, if the screws are accurate, is proportiou.-il to tlie amount
threuglijwniich the, head is turned. Each head is graduated into
100 Squal parts on the drams u and r, so that, by estimation, tlie
reading can easily be cariied to tttWIi of a revolution. The total
iruir^er of revolutions is read otf by a scale attached to the side of
tha*lBox, but not seen in the figure.
^Two' ,spidcr webs are stretched across the forks, one (() being
feniented in a fine gi-oove cut in the iniiei- fork k; the other (s) in a
similar groove cut in the outer fork I. These grooves arc sinuiltane-
onsly cut in situ by the maker, with the aid of an engine capable
of ruling fine straight lines, so tliat the webs when aceur.vtely laid
in the grooves are perfectly parallel. A wire st is stretched across
the centre of the field, perpemlicular to tlio p.arallel wires. Each
movable- web must pass the other without coming in contact with
it or the fixed wire, and without rubbing on ai^ part of the brass-
work. S- Should either fault occur (technically called "fiddling") it
is fatal to accurate measurement. ' One of the most essential jioints
in a' good micrometer is that all the webs shall be so nearly in tlie
same plane as to be well in focus together under the highest powers
used, and at the same time absolutely free from "fiddling." For
measuring position angles a -brass circle <jh (fig. 3), fi.Ked to the tele-
scope by the screw i, has rack teeth on its circumferem.e that receive
the teeth of an endless screw it, which, being fi.\ed by the anus xx
to the oblong box iiiu, gives the latter a motion of rotation round
the axi', of tlie telescope ; an index upon this box points out on
the graduated circle j/i the angular rotatiou of the instrument,"
\ I The English micrometer still
retains the essential features of
Troughton's original construc-
tion ft above described. The
latery English . artists have
BOBiewhat chau^
bfjj^communicati
tho^slides, . by '..n,,.,.,..,- inu ,,,, ,,,„., ,„,.,„. ^
screws, permanently to,;..thc,"^^™'i"™
micrometer head and tapping
each micrometer screw into
its slide. Instead of nmking
th&t shoulder of the sciVw' a
(latibearing surface,- they have^ ..'*'»'''''^
^ivciuthc screw a spherical bearing resting in a hollow cono (fig?'
i) atrtched to the eml of the box. . The French artists still retain
Trofl^hton's form.", Simnis (Troughton's successor) and Cooke (of
Voik)!ffoV symmetry and more cflcctual elimination of " the loss of
lime "''Yeallrd by the Germans " todter Gang," and sometimes in
P.nirUah. 'MiacJj-iash"), have provided .two pins vith spiral springs,
' Tins 13 Known os natr.sticn'8 cye-plccfl' ft was made origlnaUy by Iiim.
igcd the mode ' ^^^Wi:^
ing motion to 3 p
■attacbiu" the _^ R^
1 like q and T (fig. 2), one on each side of the screw which moves
each slide.
Crubb of Dublin, with the intention of avoiding the variation of
pressure exerted by the spiral springs when the slide is ot diUereut
distances from the head of
tlv! screiv, h.as adopted the
fvllowiug pl.in. Where the
screw enters the slide he has
a until attached to a strong
spring pp (fig. 5), the pres-
sure of which exerts a con-
stant tiusiou in the axis of
the screw, tending to bring
-the threads into close con-
tact, in opposit; directions,
with their bearings iu the
>.nt ,1 and the sli^e q. The
pressure of this spring is
regulated by the screws 5, 5,
tapped into the tliickenid
ends of the springs. For
iiiaiutainiiig the spheiical
shoulder of the screw in
close and constant I'l-essurc
on its conical bearing he
has attached a conical bear
ing to the spring j>'y/ (fig,
C). The pressure of this
on the upper part of the
spherical shoulder is regu-
lated by the screws s\ s\
passing through elongated
holes in the s]ning;i'//, and
tapped iuto tli« end of the
box.
-. The screws of micrometers are generally made witli 50 or 100
threads to the inch. Troughton's method of reading the numb--
of whole revolutions by a silver scale is inconvenieut, because r^i\
or even ;Vtli of an inch is too small a quantity to read easily ^ith
the naked eye, especially with the faint illumination tliat iVSj
desirable to use when measuring faint objects. Diffeicnt method?,
iucliidiug tho "comb" (see bebjw) and various kinds of "counters,"
have been iutroduecd with more or less success ; but recently the
Repsolds of Hamburg have ^^^
Fig. 7.
o[;=;]g
contrived a plan at once
simple and so efficient that
it will be unnecessary to
describe those methods which
this plan is certain to sujier-
scde (see below, typo D).
Grubb has introduced a
modification in the form of "=• "•
the slides with a view to .avoid the friction of one slide against thj
other. On the inner side of the brass j^late which forms the bottom
of the box (i.e., the side opposite to the cyc-piecc) four V-shaped
furrows are placed (fig. 7); and at each end of the slides are pro-
jections (fig. 8, end view) which fit into these furrows. The slidce
are kept down in their places by springs attached to them, whic'b
pre-ss upon the inner side of the lid of tlic box.
Troughton's mode of giving rotation to the position circle is now
abandoned. A iniicli quicker motion in position angle than can
be obtained without slow motion is often desirable, since, in
observing very close double stars, the unCi rtainty of each point-
ing may amount to several degrees iu the most accurate measure-
iiRUts The plm of a pinion working iu a toothed wheel is
ofleu emplo}ed but that also is too slow. Most modern micro-
in ttrs ai now fitted uiih a clamp and slow motion screw (sec fig.
^ tj 1 e B) Tills permits observation of tu)sition angles of veiy
close objects bj simple rotation of the box with the hand ; while the
^lou motion, after clamping, j^crmits the more delicate mo\ement3
tl it lie lequucd in measuring tho position angle of objects f.irther
ipit
The Cookes and Grubb have for ye.irs almost invariably trans-
f lud the position circle from the micrometer to the telescope tube.
The whol e\e end with its focussing airnngeincnts rotates, and \\.^
lotition can be measured by a ciulo attached to the butt end of
the tube rheie is considerable convenionce iu this arrangement
One position circle only is reqirfied for all tlie micronictci-s that
may be employed with the instrument ; and the orientation of
reticulated diaidiragms, or tho adjustment of the direction of the
slit of a spectroscope, may also be accomplished by the same means.
Uut, after a very extended experience of all the various ty|vs of
existing inoniitiug>, the picseut writer does not hii.itale to express a
deei.led jnefcrence for a ]io.nitiou circle attached to tSe micrometerand
a rigidattaehmcnt of the eyc-eud to the telescope tube,— liaviug never
seen an eye-end attaehed'to a position circle on the butt end of the
telescope-tube in whi-h, a'tor 'ho wear and tear of a few years,
■MICROMETER.]
MICRO jMETER
245
Frann-
hofer's
Slar
mioro
mttcr.
.„n,A lnn«ness or shake could not be detected. This is a fatal fuult,
Wciallvia those delicate observations of differenoo of do.hn.^
•J^ \.w.hh^ve latterly formed so ilrominent a feature in refuied
tion "■•''f.''\7';;,,'yoQ the other hand, in some Rood old micro-
m.crometr.e researc . O"';; °" "^^ if Good Hope, that are
SlXuVimdrelf VSr^Ses, tl'Jcre is no trace of shake or
''^1h:'mIcrolL""f°t;,>fB represented in fig. 9> is the original
MeV mTcrometer of the'cape Observatory, n.ade on rnnnhof s
model • S is the head of the micrometer screw proper, s that of the
S?ew movinK the slide to which the so-called ' fi.ved ^^eb is
Xche^r/ that of a screw which moves the eye-piece E. C .s th
clamp and M the slow motion m position angle L, L are
Sat?ached to a larger tube N ;. the '?"" / ' '^f ^ ^"
» stron" hollow cylinder which terminates m the screw V. By
?hU scr?w the whole apmratus is attached to the telescope. The
Fig. 9.
iio2zle3 of sm.-ill lamps are inserted in the tubes L, L, for iUu-
minatin" the webs in a dark field ; the light rem these lamps is
admUeS through apertures in the strong hollow cylinder above
n'enoned (for" illumination, see below).^ In this micrometer
?he three slides moved by S, s, and s' arc simple doveta Is
The lowest of these slides reposes upon a foundat on-plate «.,
into one end of which the screw s is tapped. lu the '"'JJlo »
this slide a stiffly fitting brass disk is inserted, to which a smaU
turn-table motion may be communicated by ..n attached arm, acted
on bT two fine opposing screws accessible to the astronomer , ami by
?heii- means the '"fixld wive" may be rendereJ strictly parallel
with the movable wire. , . ..
The micrometer screw ismounted on the s ide which cavr.es he
movable web. Fig. 10 shows a plan of this slide; the duided
(lv«m of the scvew is omitted for sake of clearness. Ihe
screw S has a shoulder at h, carefully fitted and ground to a
bearing so as to work sweetly in a hole in the very strong spring
cr; the otlier extremity of the screw is formed into a pivot, « Inch
fits a hole in the brass piece $$. The end of this piyot-hardcned,
iiolished, and slightly rounded— rests on the flat surface ot an agate
a wliich is imbedded in the end of the slide, and kept firmly in its
piace by the brass piece e^. By cai'eful adjustment of the screws
e $ sulticieJit pressure may be left upon k to slightly bend tlie strong
sprin" (T<r and thus eliminate all end-shake without preventing easy
action of the screw. Tlie screw passes at tlie
same time through the bush B (shown in
plan and elevation, fig. 10) attached to pr
(fig. 9) ; and there is a fine saw cut, wliieli
tan be narrowed by the small screw t,
■ " ■' ■ ' """ IlE;
astronomy have been executed. In this micrometer the s"ew » i»
mounted; on its own slide and has a divided head precisely like
the screw S (fig. 9). The plate rP is elongated towards s, and tlie
corresponding bush B is attached to this elongation The screw y
is shifted to another part of the eye-piece slide, so that it do" not
intevfcvo with the incveased diametev of the scvew s. Fvaunhoters
micvometer in this form belongs to type A, but is quoted under
tyiie B for convenience of descriiition. r. a 1,
It is not necessary to give a figure representing type (-■. ^ sucn
micrometers have been generally constructed on Tronghtons type
(fi''s 12 3) with the omission of one of the screws, ami witii
one ov move of the modifications descvibed in detail under type A.
Some have also been made similar otherwise to the Fvaunhofev con-
stvuction, by omitting the screw s with its corresponding slide
and attaching the fixed wire to a circular plate m ;v'. ,
GoodTnst vSments have been made on type C by Clark (Cambridge a.A,
Jlassachusetts), bv Steinheil (Munich), and by the gve.it French filar<,
aitistsTcretai F:-oment, Brunner, Eichcns; and good work has been micrw
done l^th ?hem. Ent it is necessary that the ervovs of the screw met«S
should be very carefully determined since, in tj-pe C such eiro 3
cannot be eliminated by employing different par s of the sciew to
n.easure the same angle. There is a °o'";;°'^«iy descv nt.on of
micrometer that forms a link between types C and D, of which the
n ost amons example (by Clark) isattaehed to the gjf^t Washmg-
ton telescope. It is essentially a micrometer of type C with a slida
0 folk and a scvew of the English foim of construction But the
"istninient is provided with a screw as at . (fig. 9 , ^h'ch ius^.«l
of changing the position of the fixed wire, moves the whole n^ao-
meter box fn the direction of the axis of the measnnng screw. Thus
the fixed wive can be set exactly on one stav by tho screw s w hi e
he other star is immediately afterwards bisected by the movable
wire and that without disturbing the reading for coincidence
of the wires. No one, unless he las previously worked without
such an arrangement, can fully appreciate the '^dvantageo bung-
in" up a star to bisection by the fixed wive by moving the ""oi ometer
box with a delicate scvew-motion, instead of having to change the
direction of the axis of a huge telescope for the same purpose
AVhen it is fuvther remembered that the earlier telescopes were not
provided with the modern slow motions in "gbt ascension and
that the Struves, in their gigantic labours among the double stars
u ed to complete their bisections on the fixed wive by a p^ssuve of
the finger on the side of the tube one is fueled whether mo to
' wonder at th^poor adaptation of means to ends or the man ellous
patience and skill which, with such means led to « <^h W^'?- "
should be added that Dawes practically adopted a ';'oJ;^<^^t.on of
Clark'.s micrometer by using a sln'l»"g Piece. and bolting one of
the heads of his micrometer {Mem. E. AS., vol. Y^V.J'.liJe,
His slipping piece gave motion Jo the niicrometer by two sUdes
one in right ascension the other in decimation, so that " eithei of
the webs can be placed upon dthcr of the components of a double
star with ease and certainty." . {k,.,..„j
All micrometers used, in conjunction with a m.croscore, f6"«Jd-
ing the divisions of transit circles, hcliometer sc^es,«:c., are of the
type C. The reading micj-ometer is shown m fig. 11. C is tno
^ ' objective, D the micrometer box, E the grad-
-t nated head of the screw, G the nulled head
hv which the screw cc is turned, A an ej'c-
piece slidina in a tube B, aa (fig. 12) the slide.l
close tho bush upon the micrometer screw ,JroS\-, ,
with a view of pveventing "loss of time."
The spidev web u, is cemented on the fuvthet
side o£ the thin plate vi^y, the vavnish being
applied in the countersunk holes shown by
the dotted circles ii, /n. The slide is counter-
sunk to about half its thickness within the
area indicated by oooo, in order to allow the
adapter of the cyc-jiiece to come sufficiently
close to tho webs. The eye-piece was origin-
ally moved by a pinion wovkiug in a rack r
(fig. 9); but the screw s* ajiplicd by Simms
was found by ilaclear to be more convenient p. j^
for the pnviwse. Beyond this, and tHegrad- *' '. . .
uation of the edge of the circle witli more strongly cut divisions
than those ovigiually engvaved on the face of the civclc, the in.stvn-
ment vcmains and is figured in its original form. Tistor and
Martins (Bevliu) havo also made excellent instvumcuts of the
above type. There is a celebrated micrometer of their make, with
IDunsluk which, in the hands of Brunnow at Dunsink (Dubhn), some of ,
micro. tl;e most perfect and refined investigalions ever made m ]>ractical I
Uneter. , ^-^,.„ „ i, remcmbcrcl Hint llic mcasurcmcms . ( tlic Sir
ScccM tlic Bonds, Maclcnv. and of most niodi-rn CoiUinc
• Ixcn ni-iJ^- Mitli Fnuiilioltr or Mora nilcromctcvs, it is no
flc 9 rppivsonft tlie instrument withwhicli tlirce-fourll
I o( tlic l*«t rtdy years iiave.bccn made.
.. Dcmbuwskl,
inoiiicrs Jiiivc
■I, to say mat
. Fig. 11. f 'S- 1"
and h, b the spiral springs. The focal length of the ohjective
and the distance between the optical centre of the lens and the
webs are so arranged that images of the divisions ave formeiJ ni
the idane of the webs, and the pitch of the scvew is such that oue
division of the .scale covrespouds with some whole number of re^
volutions of the screw. i i •„ »v;
There is what U technically called a "comb iiisevted m tho
micvometcv box at il (fig. l-2),-its upper surface being nearly in the
i.lane of the wires. This comb docs not move with rcfercnrc to the
box, and serves to indicate the -ivhole revolution of whicua fvac ion
is read on the head. In fig. li a division is vepresented bisected by
cross webs, and five revolutions of the screw corresi^ond Mih one
division of the .s.-alc. In all luoden. reading micrometers tbe "o"
webs of fig. 12 are replaced by parallel webseiybvacing the dmsion,
"TTlicla.e r.>,l.:S~.7\xZ^.n n^J\ "> say, quaintly and iii.l. Ivulli, ••After «%'
the best pail ol Ibe ■■■i. --."»•" u .l,o man at Hie snuU end.
246
MICROMETER
[lyrcs OF filak
(fig. 13). The means for chauging the length of tli«[tube and the
distance of C from the scale are omitted in the figur^llftt'hese apf li-
auces are required if the ""run" has to be accurately
adjusted. By " run " is meant the difference between the
intended whole number of screw-revolutions and the
actual measure of the space between two adjacent di-
visiona of the scale in turns of thp screw divided by the
number of intended revolutions. Indelicate researches
two divisions of the scale should always be read, not ' '8' ^^' ,
merely for increased accuracy but to obtain ^the corrections for
"run ' from the observations themselves.
Bepsold's Fig. 1 4 represents an important type of reading micrometer by the
reading Ropsolds. Here the web-frame is mounted on the screw itself The
micro- limiting plane of motion is at }), where the end of the micrometer
^eter. screw bears upon the hardened, flattened end of the screw s, and is
kept in l>earing against this plane by the spiral spring q. Rotation
Micro-
meter
errors.
Fig. U.
of the wire-frame is prevented by the small stud m which passes
through the *eb-frame and projects slightly on both sides of it,
just barely touching the inner surfaces of the top and bottom of the
. micrometer box. The web-frame thus rests solely on the screw and
on the point m, and therefore follows it absolutely and accurately.
nThe comparative merits of the various micrometers are discussed
by Lord Lindsay and Mr Gill {Dunecht Publications, t61. ii. pp.
'53-55, 1877). If the screw of the Repsold micrometer is bent, so
that, for example, the end of the frame next the screw-head is raised
and that next the end jo lowered, a twist will be given to the web-
frarae, and th& centre of the wire will be moved nearer to the micro-
■meter head than it should be, while the reverse effect will follow when
,the head has been turned through 180°. The eflect of a similar
error on the other micrometers described would be of a much less
Amount. They are, however, liable to errors of another character. ■
'If, as in Troughton's original micrometer, the shoulder is square,
the hole in the end of the box may be left sufficiently wide to allow
for a small error in the parallelism of the screw-matrix with the
motion of the slide, but the smallest bend in the screw causes the
shoulder no longer to bear fiat, but to ride ou its-edge, thus intro-
ducing an extremely uncertain form of error. If the shoulder is
spherical, fitting into a hollow cone on tlie end of the box, as in tlie
micrometers of Simms, Cooke, and Grubb, an almost inconceivable
accuracy of construction is implied in drilling the matrix of the
screw in the slide so that its axis and that of the cone shall be in
tKe same straight line, and both parallel to the motion of a point
in the slide. Any departure from perfect accuracy iji this respect
has the effect of bringing different portions of the spherical shoulder
to bear on different parts of the cone for different revolutions, and
introduces errors of a character by no means easy to deal with. In
addition to these objections there always is the greater objection
of employing as a delicate contact-measuring surface one that is
exposed where oil is used. Dust and oil will arrange themselves in
layers of variable and uncertain thickness and defeat all attempts
to secure absolutely consistent results. In Repsold's micrometer
the poiiU d'appui is a small hardened and polished bearing, requir-
ing little lubrication, and perfectly protected from dust; the errors
of 'the screw (some of thera exaggerated, certainly) are faithfully
reproduced, and consequently determinable, and beyond this the
jwork to be done by the screw is reduced to a minimum, — no slide-
frictiou having to be overcome. If we are to regard as the most
perfect instrument, "not that which has absolutely the smallest
errors, but that which rfproduces its errors with the most perfect
consistency," undoubtedly Repsold's foriif of micrometer is best.
In order to avoid the exaggeration of the screw-errors produced
by the non-symmetrical position of. the screw in Repsold s micro-
meter, Stone, in December 1879, exhiwrted at the Royal Astronomical
Society, and described [Month!!/ Notices, p. 270), a modification of
Ropsold's instrument. But, both in his statement of the compara-
tive merits of the Troughton ana Repsold micrometers and in the
•new form which ho figures, Stone overlooks a strong point in the Rep-
lindaay- sold form, and in that proposed by Lord Lindsay and Gill three years
GHU mi- previously,' — namely, the avoidance of all friction of the slide, and
urometer, the elimination of all error or strain that may occur from a want of
parallelism in the axis -of the matrix and the motion of the slide.
jThe Lindsay-Gill micrometer will be better understood from the
following description. In hg. 15 Ss is the micrometer screw; its
1 J>umcht Publkationi, vol. U., footnote p. hi, Dimecht, 1877. ~^
cylindrical axis is nicely ground to fit a hole in the side of the box
at « ;- the same axis, but ground to a somewhat smaller cylinder,
fits neatly but smoothly a hole in the web-fiame att. , A screw,
cut on the same axis, is tapped into the web-'
frame at «, and the axis terminates in a pivot
which fits a hole in a brass plate cc. The end
of the piyot— bardened and sligbtly rounded
— rests on a flat agate ^ bearing o, which is
imbedded in the plate B, and securely held
in silu by pressure of the plate cc. ■ The platu
B is firmly attached to the bottom of the
box. q, q are spiral springs mounted on pins,,
Both springs and pin pass freely through tli^
web-frame a.t p, p, and the pins (but not the
springs) pass freely through the frame at n, «.'
The parallel webs for observing the division
(fig. 13) are mounted on the forked end of
the frame at ww.
The web-frame is' narrower ana tiiinner
than the breadth and height of the interior
of the box, and is only prevented from rotat-
ing by the delicate touch of the projecting
ends of the pin m on the inner surfaces of the
top and bottom of the box. It appears that
a frame so mounted fulfils all theoretical con-
ditions of accuracy. It is perfectly free to
follow the motion of the screw and accurately
.to reproduce its errors, notwithstanding any
reasonable faults of workmanship ; and no
permissible shako or fouling of the bearing ' ■'" ^'8- ^^■
at a can produce sensible error in the distance between the bearing
surface of the agate plane and the spider webs. The motion is pro-j
duced with the minimum of friction; and the "feel" of t^e screw
is therefore as delicate and perfect as it is possible to make it.
The micrometer of type D shown in fig.y 16 has ^recently
been made by the Repsolds for the Cape Observatory. .^ As this
instrument combines
all tl;eir most recent ^
modifications, we de-
scribe it in detail.
Fig. 17 represents the
same micrometer with
the upper side of the
box removed. '. The
letters in the descrip-
tion refer . tp^ both
figures.
S is the head of the
micrometer screw, j
that of the screw by
which the micrometer
box is moved relative
to the plate/(fig. 16),
s' that of the screw
which moves tlie eye-
piece slide. . K is the
clamp .in '' position
angle, P the slow mo-
tion screw in position
angle ; pp is the posi-
tion circle, R, R its
two reatlei-s. The lat-
ter are in fact little
microscopes carrying pj ig
a vernier etched on °'
glass, in lieu of a filar -micrometer. These verniers can be read t>
1', and estimated to 0''2. D is the drumhead which gives the frao-
tion of a revolution, d that which gives the whole number of revo-
lution-s, I is the index or pointer at which both drums are read.
This index is shown in fig. 17, but only its mode of attachment (X,'
fig. 17) in fig. 16. The teeth of the pinion :, fig. 17, are cut on the
axis of the micrometer screw. * The drum d and its attached tooth-
wheel are ground to turn smoothly on the axis of the sci-ew. The
pinion s and the^oothed wheel d are connected by an intermediate
wheel and pinion 'V; the numbers of teeth in the w heels and pinions
are so proportioned that twenty-four revolutions of thp micrometer
screw jirouuce one revolution of the drum and wheel ff. (This is
the description of Repsold's counter referred to under typo A. ) The
divisions of both drums are conveniently read, simultaneously, by
- Tliero would be some ndvanUffO la allowltv the screV* axis to paas wUli ft
mtle Blioko llirouBli tlio liolo In llic end of tho box at a, «nd tticiTscxtendlng the
lingth of ttio larger cylinder, transfer the bcnrliiR from o to a vcll-BtllnR hole la
a picco nxrd llko B to tho bottom of tho box. This form »pouia also give aomo
fnclllllea of construction, and all tho oiled surfaces «oulJ ha ftitcctly protected.
3 Sapphire Is better ; tho agate hearing of such a scnfw has been found T^iy
tcnslbly worn.
• If It Is desired to prevent possible contact of .these \>\Dfi wfth the frame, tUft
ends of the pint may be made to enter guiding holes In a.
WICKOMETER.]
M-rC il O METER
247
^, liHia t ■ at nielit tb« lamp which iUaminatcs the webs and.flie
w'itiTu circle aUo illuminates the drur-.rhe«(ls (see on illumination
Cow) Wi» the web.frame.(fig. 17„ ^yi^ a single rod copsistinfe'
cf two cySrs accurately fitting in the ends of the micrometer
box theCger cylinder being at 0. There is a hole in the web-
ft-ame which smoothly fits the larger cylinder at fi!, and another
which similarly fits tie smaller cylinder at y' A spiral spring
Toi d round the cylinder y, resting one end on the "'"'"f ' ''°™"d^
by the difference it the diameters of the cylinders fl and y and the
oUi r onthe inside of the web-frame, pre^es the latter ""'•""""^'y
towards ■» Contact of the web-frame of the micrometer with the
ride of the box at y would therefore take i;lace were 't "ft for the
micrometer screw. This screw fits neatly in the end of the box at
" p!^es loosely through the web-frame at .', is tapped into the
(reSTat f, and its end resti on a flat hardened surface at f. Rota-
"n of the web-frame about Py is prevented by the headB of the
«!rews at m ; the head of the screw on the lower side of the rame
renoses on the plane rv, that on the upper side (fg. 17) touches
"gCy on the inner surface of the lid of the box Such rotation
can obTiously be controlled within limits that need not be further
coMidered. But freedom of. rotation in the plane of the paper
Fid.*
ffig. 17) is only prevented by goa(ttlM\\s of the holes /J", 7'; and,
since the weight of the slide is on one side of the screw, misfit here
will have the effect of changing the reading for coincidence of the
moi able with the fixed web in reverse positions of the microniater.
With the Cape micrometer a systematic difference has been found in
the coincidence point for head above and head Ije'.off ainouoting to
9"-14. This corresponds, in the Cape instrumcut, with an excess of
the diametereof the holes ovorthcsa of the cylinders of about ,^W1>
of an inch,— a quantity so small as to imply good workoiaijship,
though it involves a systematic error whioh is verv much larger
than the probable error of a single determination of the coincidence
point. The obvious remedy is to make all measures on opposite
sides of the fixed web before reversing in position angle,— a precau-
tion, however, which no careful observer would neglect. In measur-
ing differences of declination, whore the stars are brought up by the
diurnal motion, this precaution cannot be adopted, because it is
necessary always to bisect the preceding star with the fixed web.
But in AS measures index error can always be eliminated by
fcisecting both stars with the same web (or different webs of known
interval fixed on the same frame), and not cmidoying the fixed web
>t all. Had the spring 7 been nlaced as in fig. 14. and the cylinders
e and y been made to bear lik« the pivots of a transit on seg-
menUl bearings in the frame at jB' and y', it is probable that the
difference in coincidence points would not have existed. Such a
modificatiou appears advisable, unleea this construction, by leaving
the end m tjss free, should make the " fed " of the screw less sweet
«nd perfect The discordance in zero when known to exist is
nsUy of no conncquencc, because tlie observ&liojis can be so
arranged as to eliminate it. ' ---
The box is mounted on a strong hoUoWsteel cylinder CO (fig. 17)
by holes n, « in the endspf the box, which fit the cylinder closely
and smoothly. The cylinder is rigidly fixed in the studs C, C, and
these are attached to the foundation plate/. The cylinder contains
« towards j| a sliding rod, and towards 9 a conipres.std spiral spring.
There is thus a thrust outwards of the spring upon the hollow cap
W (attached outside the box), aad a thrust of the rod upon the end
of the screw ». The position of the box relative to the plate/, in
the direction of measurement, depends therefore on the distance
between the end of the screw s and the fixed stud C. A screwing
in of » thus causes the box to move to the left, and vice tersa.
Rotation of the box round CC is prevented by downward pressure
of the spring Z on a projection attached to the side of the box. The
amount of this pressure is regulated by the screw /.
The short screw whose divided milled head is <r shifts the zero
of the micrometer by pushing, without turning, the short sliding
rod whose flat end forms the point cCappai of tlie micrometer screw
at f The pitch of the screw a is the same as that of the measuring
screw (50 threads to the inch), and its motion can be limited by a
stop to half a revolution.
The five fixed webs are attached to the table tt, which is secured
to the bottom of the box by the screws p. The throe movable
webs are attached to the projections \\ on the frame aa. The plane
jburfaces tt and AA are composed of a bronze of very close texture,
"which appears capable of receiving a finish having almost the truth
and polish of an optical surface. It seems also to take a very clean
V cut, as the webs can be laid in their fnrrows with an astonishing
ease and precision. These furrows have apparently been cut tii sila
with a very accurate engine ; for not the slightest departure from
parallelism can be detected in any of the movable webs relative to
the fixed webs. Extraordinary care has evidently been bestowed
in adjustin" the parallelism and distance of the planes t and \, so
that the movable wires shall almost, but not quite, touch the sur-
face T. The varnish to fix the \yebs is applied, not on the surface
T as is usual, but on a bevel for the purpose,' the position of the
webs depending on their tension to keep them in their furrows.
The result is that no traco of "fiddling" exisU, and the inoT-
able and fixed webs come sharply together in focus with the highest
powera. Under such powers the webs can be brought into apparent
contact with such precision and delicacy that the uncertainty of
measurement seems t> lie as much in tlie estimation of the frac
tion of the division of the head as in the accuracy of the contact.
It is a convenient feature in Kcpsold's micrometer that the webs are
very near the inner surface of the top of the box, so Uiat the eye is not
brought inconveniently close to the plate when high powei-s are used. _
Jliciometers of the typo E have been invented by Alvan Clark and Clark s
Onibb Clark's micrometer was exhibited at the Juno meeting of mBro-
the Hoyta Astronomical Society in 1859 {ilonthhj Kolias E. A. S., meter f
vol «ix.). It is capable of measuring angles up to about one degree, large
O is " furnished with two eye-pieces, composed of small single angles,
leasaa, mounted in separate frames, which slide in a groove and
can be separated to the required distance. A fromc carrying two
parallel spider linos, each mounted separately with its own micro-
meter screw, slMos in a dovetailed groove in front of the eye-pieces ;
and by a free motion in this frame each web can be brought opposite
its> own eye-lens. In using this micrometer, the first step is to set the
Bosition-vernier to the approximate position of the objects to be
measured. Then the eye-lenses are scparatad tiU ec h is opposite ita
own object. The frams containing the webs and their micrometer
screws is then slid into iU plaCB ; and the webs, having been
separated nearly to their proper distance by their free motion in the
frame, are placed precisely on the objects by their fine screws the,
oI»erver's eye being carried rapidly from one cye-lcns to the other a
few times, till he is satisfied of the bisection of each of the objects by
its own web. The frame is then removed for reading off the measure
by means of an achromatic microicopc, on the stoge of which it is
placed." .The advantages which Clark claims a« those :- J
" 1. Kstanccs can be observed with great accuracy up to about
one dcgroe, and the angles of position also. , , , , ■
"0 The webs, being in the same plane, are perfectly free from
naraUax, and are both equally distinct, however high the magnify^
mg power may be. ,. . , , 1
•'3. The webs are also free from distortion and from colour.
'"4 A different msgnifying jiowcr may be used on each of the
object's,— which may be advantageous in comparing a faint comet
* 'it aVpcars to us that the method of removing a slide in order to
measure the interval between the webs U liable to objection not
only because of the risk to the webs, bnt because the taking
of measurements of such a different character with a different
instrument is inconvenient and troublesome It is true th.it the
intervals between the webs could be measured by an assistant, and
two or more different slides be employed to sore time ; but astrono-
mers will probably generally prafer the method introduced by
Grubb described below. It is understood that Clark has since
improved this instrument by an ingenious arrangement oJ prisms,
which permits both webs, even though separated one degree in a
laroe telescope, to be seen in the same eye-piece. The arr.iugement
is not describe4, and is said to be, as yet, somewhat troublesome
to arronge previous to measurement, though when
anged jj
^M^lscUntifil'' r-^mli>>0> of Royal Dublin So<icUl)J^^^^^
applied »1U lie seen !" fls "
248
M I C R O M E T Em-
[WEBBIKO.
Grubb'^rf what he calls his "duplex micrometer," shown in pprspectire in fi^
^upU^ 18 : — " A plate of glass about 2^ inches Btjuare is ruled with twenty-
micro- one lines in one direction j\th in .h apart, and two lines iu tlie other
meter. direction 2 inches apart. The extreme lines of the set therefore
form a perfect square of 2 inches. These lines are ruled with
exceeding accuracy and care, but provision is left for ascertaining
any errors that rcmnia either as to distance or want of perfect
squareness. Along
one side of the square
is mounted a micro-
meter frame in the
ordinary way, actu-
Bted by a screw of
one hundred threads
to the inch. This
micrometer frame
carries eleven lines
corresponding exact-
ly to each alternati
line in the glast
reticule, sothatwhen
the first spider lino
is made coincident
with the first dia-
mond line on the
glass the last spider .
line will be coincident with the last line on the glass, and each of
the spider lines will be coincident with all the odd numbers of
diamond lines, 1, 3, 5, 7, 9, 11, 13, 15, 17, 19, 21. Over this glass
plate is placed a brass cap in which two eyepieces are mounted,
one sliding in a groove at right angles to the other,— so that,
while one has its journey backwards and forwards on the horizontal
line, the other has its journey on the vortical line, according to
how the cap is placed, for this cap is capable of rotation to meet
arious circumstances.
■ "How to Use the Instrument— \. The two stars are brought on the
horizontal line, and the distance measured from centre to centre
■long that line. This distance is measured by counting the number
of spaces on the glass, adding the residue as measured by the
micrometer screw. Thus the screw is never used for larger measures
than ^th inch, and therefore errors of screw and temperature eiTors
are much reduced. In bisecting, one star is brought into the "field
of one eye-piece, and a bisection is made with one of the diamond
lines by moving the micrometer by one or other of its slipping piece
screws. Then the other eye-piece is moved till the second star is
seen, and a bisection is made with the nearest spider line by moving
the micrometer head. Then the eye can be moved back to the first
eye-piece, and the bisection checked, and again back to the other
eye-piece. When it is seen that both are eatisfactory the measure
can be read off. 2. The micrometer is turned round till the
horizontal line becomes parallel to the path of apparent motion of
the star. This is easily found by stepping the clock and allowing
the star to run along the horizontal wire. Now the other star wifi
be found to cross the vertical line somewhere, while the first star is
OQ the horizontal line. This second star is then bisected on the
vertical line, while the first star is bisected by one of the spider
lines ; thtis the difference in right ascension is found. We then
have two sides of a right-angled triangle and of course all the
elements are known.
" To Ascertain the Errors {if any) of the Distance of the Lines. —
Of course, the usual plan of taking transits can be adopted, and to
ascertain if the lines he perfectly ut right angles a special additional
eye-piece is provided, so that transits can be taken across each
diagonal of the square."
! This instrument has great advantage over Clark's in ease of
adjustment and use, and has done good work at the University
Observatory, Oxford {Mem. R. A. S., vol. xlvii. pp. 5-12).
Professor Pritchard claims too much when he estimates its work as
equal in accuracy with that of the heliometer— at least the pnbliehed
results do not confirm such a view. But it is a very valuable
instrument for measuring objects too faint for the limited aperture
of most heliometers, and which at the same time are farther apart
than the field of view of an ordinary eyepiece.
The accuracy of the duplex micrometer would be very greatly
increased if Clark's idea (above mentioned) of viewing both widely
separated webs in one t-ye-pieco of high flower could be reduced to
a convenient practical form.
Method of Webbing the Filar Micrometer.
.The webbing of a micrometer is a process that should be familiar
to all practical astronomers. English opticians usually proceed as
follows. A spider (the variety ia marked by a cross on the back,
and ia found in English gardens about decayed wood) is cauglit,
and placed on a wire fork. The insect immediately ottnches a web
tothe wire and begins to lower itself by a web to the gTOund. This
web is wound up on tho fork till ten or twelve turns, separated by
A convenient space, have been secured. . A brush with vamlBh is
then passed nlong the prongs ; the webs are thus securely fixed to
the fork. The parallel prongs of the fork munt Lc sufficiently far
apart to allow tho web-framo of the micrometer to pass between
them. The frame to be webbed is placed on a flat dull black
surface between the prongs of the fork, the latter being carefully
arranged so that one of the webs lies nearly in the furrow ruled id
the frame for its reception. As the web-frame is generally thicker
than the fork, the web will now be stretched across the former,
with a certain amount of tension, and is brought into the furrow
with a finely pointed piece of soft wood. If the surface of the fian>e
i? well polished, and the furrows sharply cut, without "burr," the
web should lean shari-ly and decidedly into its place. Each end
of the web is then secured by a drop of shellac varnish, which
should be allowed to hnrden thoroughly before the frame is touched.
'I'he webs can be vary readily so handled against a black back-
ground, wifti tho aid of a hand lens of 2 or 3 inches focus. In
experienced hands thismetliod gives good results, but the following,
which is generally followed on the Continent, is preferable.
A web, about 2 inches longer than tlie wiJth of tho frame, is
unwound from a cocoon,' and small pieces of lead are attached
to its extremities by beeswax. One end of the web, with its
attached lead, is laid on a piece of cork floatijig in a tumbler of
water ; the other end is allowed to hang down in the water, where
it becomes thoroughly saturated and untwisted. It is then laid
across the fork, and dropped into its funows in the manner above
desL-ribed, the little lead weights exerting a definite tension.
V^ijnish- is immediately applied to secure the webs, and the frame
is not touched till it is dry. -^
The bevel-edge of the web-frame introduced by Repsold (type
D) offers great facilities for accurate webbing, and should be em-i
ployed in all future micrometers.
Hhimination of Micrometers.
When micrometer observatious are made by night it is necessary
to have some mode of rendering the webs visible, — either by rays
of light at right angles to the axis illuminating the webs, or by
rays nearly coincident with the axis of tho telescope. In the
former case we get bright webs in a dark field, in the latter dark
webs on a bright field. -^jj
In the older telescopes bright web illumination is produced by
small lamps with nozzles that enter the tubes L, L (fig. 9). The
illumination is regulated in colour and intensity by wedges of
coloured or darkened glass passing through- slides in the nozzles.
But it is inconvenient to have lamps so near the observer's cyo, and
it is at least very difficult to obtain a perfectly dark field when the
wires are illuminated in this way.
The Clarks, in their micrometer of the great Washington tele-
scope, have made the end of \)oxT (fig. 15) transparent, and light is
thrown on the webs from a lamp held by an assistant. Holdcn has
very recently applied a lamp ingeniously hung so as to preserve its
verticality and the constant direction of its light in a similar way,
adding a plain silvered mirror inside the box and opposite the
lamp, so as to illuminate the webs symmotrically. In the Clarks*
and Holdcn 's methods it is only the webs at right angles to the
screw that are illuminated.
For illumination of tho field, in. very old tek-scopes, light was
thrown on a small ivory reflector fixed outside tjio object-glass in
the axis of the telescope by an arm fitting on the cell of the lens.
This ipvolved the aid of an assistant to direct lamplight ou the
ivory reflector, or the very
frequent change of a
lamp support. After-
wards the light from an
attached lamp was intro-
duced through a hole iu
the telescope-tubo and
thrawn upon an ellipti-
cal pUine {generally dull-
gilt) having its centre
part cut away sufiiciently
to avoid interruption of
the cone of rays from the
object-glass. Many in-
genious modes of sus-
pending the lamp have
oeen invented for the pur-
pose of securing a con- _. ■
atant direction of its light ' *S- l-*- ;
coupled with vertirality of the lamp. One of the best of these, due
to Cooke, is shown in fig. 19. L is the lamp, P a prism to rcflei t
irc clastic, better ihapcd, ui-l
of tho ln.'»ect"to wcupo. Tho
bpBl wubs »c bftvc scon were from a oocoon obtained -In Holland, bot we baru
been unable to aacerluln tho name of tho variety of epliler.
* Ai'fcclandcr lued to apply two dropa of vamlali at ,caoh end of Iila'wcba. Tic
nrtt fixed onch extremity by a drop of-ahrriae Tanilnii, and after thut bad drkif
ho aj'iihcd a drop of cnj.ul varnish nenrtr tiic centre of llie frnme ; tho latter look
• long time to harden, but gave ulllma'ely a tnucli btronger attachment.
.M;rC R O M E T E R
TLtUMlSATION.]
Its light into the tub^ ITTdisk t6 rcgulrSi" the quantity of light,
B a disk with glasses to regulate the colour of the light, b a
sorinz to clamp the disks, C the counterpoise of the lamp, G a
iwise to preserve the horizontality of the axis CL. But astronomers
owe to the genius of Grubb the introduction of a more efficient
and convenient system, viz., the performance of all necessary illu-
mination of an astronomical telescope by a single lamp, and the
perfect control of the illumination of the field or webs, and the
reeulation of these as to intensity or colour by simple motions from
the eye-end. It is impossible to speak too highly of Grubb s efforts
in this direction ; ^e has broken the ground in this department of
astronomical engineering, and rendered the working of so huge an
instrument as the Vienna telescope of 27 inches aperture not only
convenient, but easier for a single observer than that of a very
small telescope of the older constructions.
But in the illumination of the field wires and scales of a micro-
meter Gnibb's original method has reeently been surpassed by
one which is due to the Rcpsolds. We shaU therefore descnbc the
Fig. 20 represents the eye-end of a telescope. The reader will
recognize the micrometer (figs. 16 and 17) previously described. L
is a paraffin lamp fitting by a
bayonet joint into a copper cover
e. This effectually defends its
glass chimney against accident,
and protects the lamp from wind.
The simple means by which this
lamp is made to preserve its ver-
ticality in all positions of the
telescope is evident from the
figure. By this lamp alone the
bri"ht wire or bright field illumi-
nation is given at pleasure, and
with any desired intensity, simply
by movement of the small pin p.
The position circle and the head
of the micrometer are also illu-
minated, as well as the declina-
tion circle, by the same lamp.
AB is a cylindrical box, ending ^
in a tiTincated cone towards A. '■'
Itisshown, mid-section, inaplane
passing through the telescope axis,
in fig. 21, where all details un-
necessai-y to the explanation of the
illumination are omitted, and pro-
portion of parts is sacrificed to
clearness. P is a prism (fig. 21)
that rotates with the lamp and
reflects its li"ht into AB. Tlie
flame of the lamp is in the focus
of the lens !l, so that the rays
become parallel after passing
through it. Tliere is a sliding *^'g- •*••
motion to perfect this adjustment. There is a well-polished flat
annular reflector of speculum metal n- (fig. 21), which reflects light
upon the double minor il (fig. 20), whence it is diverted to the two
opposite points on the declination circle that are read by micrometer
microscopes from
the eye-end (the
latter are omitted
for sake of clear-
ness).
The little handle
at p' and the dotted
lines p': represent
an iris-diaphragm,
very ingeniously
constructed, mount-
ed on a plate of
transparent glass. ^
There is • flat ring ^^Js^^
of brass, canning ^^^
four pins, which
is turned by the
handle p', in a
pl&ne at right
angles to Vn.
These pins work in
spiral slot) cut in _. „.
four slides. Thus "»• "'•
rotation of the riug causes the four slides to approach or recede from
a centre. When the handle p' is in the middle of its range, the
slides together form a disk as large as the hole in the diaphragm rfrf,
249
whence it is diverted to a silvered reflector eementcd on the middle
of the inner surface of the objcct-gbss, and is then r'^flccted back
olon" the axis of the telescope to illuminate the field at to. When
p' ispushed tt the other side of its i-ange the slides approach and
oveilai> at the centre, excluding liglit from n and allowing tt to fall
upon the reflector s instead. From s the light is thrown upon the
webs a, u by reflexion from a white papier mache sui face laid on the
inside of a thin hollow brass truncated cone rx. The edge of this
cone forms the circle seen within tt in fig. 17. All stray light is
prevented by the light-guard tube vim, which is attached to and
moves with the rotating part of the micrometer. The result is to
produce a symmetrical illumination of the whole system of- webs in
a perfectly dark field. It is also obvious that by placing / at an
intermediate position between the centre and the extremes of its
range any desired modification of bright wire or bright field illu-
miiuitioii can be obtained at pleasure.
The li''ht falling on the papier mache hollow cone is intercepted
at threo°points by prisms, one of which /i is shown in section.
These prisms are inserted in the cylinder which carries the
foundation plate of the micrometer box and rotate with it. Two
of them divert light npon the reflectors (seen from different
points of view in figs. 16, 17, 20). The third prism after two
reflexions (figs. 16, 20) illuminates the micrometer head. The
whole arrangement is in the highest degree elegant, and we havo
found it most simple and convenient in practice. The screen C
(figs. 20 and 21)— made of thin copper and attached to AB — effectu-
ally protects the observer's eye from stray light fr9m the lamp.
It has been found essential, in bright field illumination, when the
highest accuracy is desired, to have the illuminating rays parallel ■
with the telescope axis.
In the best telescopes of the future some plan like that of Eeri-
sold's, above described, will doubtless be adopted. It is probable
also that with the introduction of condensers, in conjunction with
the incandescent carbon light in vacuum, electricity will ultimately
supersede the oil or paraffin lamp in illuminating astronomical
instruments. A small " Swan lamp " can be placed anywhere, is
unaffected by wind, and gives off comparatively little heat. These
are most valuable (lualities for the purpose in question.
The asti-onomer-royal (Mr Christie) has recently used luminous
paint to render the measuring pointer of the Greenwich spectroscope
visible at night This paint, after exposure during the day to sun-
light, shines at night mth a dull phosphorescence sufficient to make
the micrometer pointer, to which it is applied, faintly visible, and,
it is stated, with very satisfactorj- results.
On the nse of the filar micrometer consult Struve, Mensurx Mknmttricx. St
Petersburg. 1837; Brunnow, Prartical and Spherical Mtronomt/; Chouvenel,
Pracllcal and Spherical Altreiiomy; Bruimow, Ailronnmieal Obserealions and
Researches made at Dunsint. Dublin, ISTO. 1S73. 1S70 ; Ball, ibid.: kaiser, Leiden
Observations: and the papers of Dcmbowski in the Astronomische ^achrichfen
DoitbU-Image ilicrometers.
The discovciy of the method of makin" measures by double,
images is stated to have been first suggested by Roemer about 1678. Roemer.
But°no such suggestion occnrs in the Basis Astrotwmix of Horre-
bow (Copenhagen, 1735), which contains the only works of Roemer
that remain to us. It wctuUI appear that to Savary is due the first
invention of a micrometer for measurement by double image. His
hcliometer (describ-
ed in a paper com-
municated to the
Royal Society in
1743, and printed,
along with a lettei
from Short, in Phil, jj
Trans., 1753, p. 156)
was constructed by
cutting from a com-
plete Tens abed the
equal portions aghc
and acfe (fig. 22).
The segments gbh , <• ^ , v.„-»»
and cfi SO formed were then attached to the end of a tube having
an internal diameter represente.l by the dotted circle (hg. ii).
The width of each of the portions aylir and o<-/ cut away from
the lens was made slightly greater than the focal
length of lens x tangent of sun's greatest dia-
meter. Thus at the focus two images of the sun '
were fonned neari'y in contact as in fig. 24. The
small interval between the adjacent limbs was
then measured with a wire micrometer.
Savary also describes another form of hehometer, on the same Sawy.
principle, in which the segments aglic aud acfr are utilized by
icmenting their edges gh and ./together (fig. 25), and covenng all
except the portion indicated by the unshaded circle. Savarj ex-
presses preference for this second pla
iOO
aud makes the pertinent
slides together form a nisk- as large as tne noie m me uiapuragn c.u, ,.i«»^» , .^.^y.^ .». JT ..',;,, „v» nf tt-<l li^ht in the two
and thus prevent all light from entering the telescope tufee. When remark that in both these models the raj s of red l'^' t •" '"^ '"»
p' is pushed to one side of its range the slides move outivards leaving solar images will be next to each other, v ""; ' 7'' ; "'.'"~°i°
a square opening in the centre so that the light falls on the prism H, sun's disk more easy to be observed than tl.eMO.. r ones.
16—11'
250
MICROMETER
[double -niAa»
Fig. 27.
be mentions " hccr-usc the classes in tliese two sorts ar* somewhat
prisiniuical, but mostly those of the first model, which cjuld
therefore bear no grwt charge " (magnifying power).
A thiril niotltl proposed by Sarary consists of two coaiple;^
lenses of ^ci^iial focal length, mounted in cylinders
side by side, niid attached to a strong brws pfatQ (fig.
26). Here, in order to fulfil the purposes of the pre-
vious motlels, the distance of tlie centres of the lenses
from each other should only slightly exceed the tan-
§ent of sun's diameter x focal length of lenses,
avary dwells on the difficulty both of procuring
lenses sufficiently equal in focus and of accurately
adjusting nnd centring them.
Bou^uer. In the Mem. Acad, dc Paris, 1748, Bouguer de-
scribes an instrument which he calls a heliometer
Lalande in his Astronomic (vol. ii. p. 639) mentions
such a heliometer which had been in hia possession
from the year 1753, and of which he gives a representation on
Plate XXVIII., fi^. 186, of the same volume. Bouguer's helio-
meter was in fact similar to that of Savary's
tlrird model, with the important difference
that, instead of both object-glasses being
fixed, one of them is movable by a screw
provided with a divided head. No auxili-
ary filar micrometer was required, as in
Savary's heliometer, to measure the interval
between the limbs of two adjacent images
of the sun, it being only necessary to turn
the screw with the divided head to change
the distance between the object-glasses tul
thet^vo images of the sun are in contact as
in fig. 27. The differences of the readings
of the screw, when converted into arc, afford
the means of measuring* the variations of
the sun's apparent diameter.
^oUond. On the 4th April 17M Dollond com-
municated a paper to the Royal Society of London {Phil. Tratis.,
vol. xlviii. p. 561) in which be shows that a micrometer can be
much more easily constructed by dividing a single object-glass
through its axis than by the employment of two object-glasses.
He points out — (1) that a telescope with an object-
glass BO divided still produces a single image of
any object to which it may be directed, provided
that the optical centres of the segments are in coin-
cidence (i.e., provided the segments retain the same
relative positions to each otiier as before the glass
was cut) ; (2) that if the segments are separated
in any direction two images of the object viewed
will be produced ; (3) thi\t tlie most convenient
direction of separation for micrometric purposes is
to slide tliese straight edges one along the othe
on the margin (fig. 28) represents them: "for thus they may be
moved without suffering any false light to come in between them ;
and by this way of removing them the distance between their
centres may bo very conveniently measured, viz., by having a
vernier's division fixed to the brass work that holds one segment,
so as to slide along a scale on the
plate to which the other part of the
glass is fitted."
Dollond then points out three dif-
ferent types in which a glass so
divided and mounted may be used as
a micrometer :—
*'l. It may be fixed at the end of
a tube, of a suitable length to its
focal distance, as an object-glass, —
the other end of the tube having an
eye*gla5s fitted as nsual in astronomi-
cal telescopes.
*' 2. It may be applied to the end of a tube much
shorter than its focal distance, by having another
convex glass within the tube, to shorten the focal
distance of that which is cut in two.
**3. It may be applied to the open end of a
reflectin;^ telescope, either of the Newtonian or tlio
Coflsegiain construction."
Dollond adda his opinion thfit the third type is
"much the best and most convenient of the three" ;
yet it is the first typo that has survived the test of
time and experience, and which is in fact the modern
heliometer
Fig. 29 illustrates Dollond'a divided object-glass
heliometer of the third type. A is the end of the
reflecting telescope, upon which the adapter B is fitted.
fig. 29.
B carries
el (not seen in the figure) formed of a ring racked at the
outer edge, and fixed to the lirass plate CC, so that a pinion moved
by the handle D may tucn it into any position. Two plates P, 0,
with the attached bemi-lenses, move in slides fixed to the plate CC^
— simuUrtneous motion, in contrary directions, b.ing communicated
to them by turning the handle E, which drives a concealed pinioa
that works in the two racks seen in the highost part of the figure.
The amount of separation of the semi-lenses is measured by a scale
6 inches long, subdivided to ^t)x of an inch, and read by a vernier
on thepUter to^f^th of an inch. In pra<nical use this micrometer
has never given satisfactory results (see Jlosotti in the Efemcridc of
Milan for 1821). It must be remembered, however, that when
Dollond gave preference to this type he had not invented the
achromatic object-glass; his preference was fully justified under
these circumstances. So far as we know no heliometer with a
divided achromatic object-glass was ever made by the elder Dollond
on the principle of his first type. His son, however, made what he
called an object-glass micrometer, which was a great improvement
on the elder DoUond's second type.
In the older construction the brass mountings of the semi-lensea
obstructed the light entering the telescope in proportion to their
separation, and the images were so coloured as to prevent the use
of any but very low powers. In the later construction the movable
segments are formed from a negative achromatic lens of much larger
aperture than the object-glass of the telescope with which me
micrometer is employed ; and, for convenience in mounting, the
segments ghh and w?/ (fig. 22) are removed. In the fine example
of this instrument at the Royal Observatory, Cape of Good Hope,
the movable lenses consist of segments of the shape gack and
tacf{^^. 22) cut from a complete negative achromatic combination
of %\ inches aperture and about 41 feet fiscal length, composed of
a double concave flint lens and a double convex crown. This ie
applied to an excellent achromatic telescope of 3^ inches aperture
and 42 inches focal length. The instrument is represented ia
fig. 30 ; the same letters indicate the analogous parts of
The frame CC, moved by _
teeth on its outer edge, o
carries one of the halves*
G of the lens, and a simi-
lar frame with teeth car-
ries the other half F. A
scale %\ inches long is
fastened like an edge-bar
to the frame of the seg-
ment 0, and each, inch
is subdivided into twenty „. „,
parts, which are read otf ''S- ^^^
by a vernier to ■m'Duth of an inch, and, by estimation, this can easily
be carried to ToVffth or yii'jr^tb of an inch. The two movable frames
are imbedded in a fixed plate HH, screwed to the adapter B.
haying a circular hole in its middle equal to the diameter of the
object-glass. The slide of the segment G is moved by tumihg
the milled head to the Tight of A, and the other segment F bj
means of a rack and pinion on the opposite side, the latter being
turned from the eye-end by a handle not seen in the figure. A
screw is provided for clamping the slide of the segment G, as it
is intended that only the segment F shall be moved in making the
final bisection. There is an index attached to the slide ofO, reading
on a rough scale engraved on the plate H, which is obviously-
intended for setting the optical centre of the segment G approxi-^
mately as far from the optical axis of the telescope on one side ad
the optical centre of the segment F will be on the other side during
the intended measurement. This arrangement not only permits the
measurement of angles t\vice as great as would be possible if one
segment were fixed, but is also important in increasing the symmetry
of the measures. The vernier is placed at one end of the scale
when the optical centres of the segments are in coincidence, and is
provided with screws at 1, which are intended for adjusting the
zero of the scale. The younger Dollond has in this model retro-
graded, in some respects, from the admirable example of his father,
who, OS shown in fig. 29, not only gave the lenses autoraatifl
opposite motion symmetrically with i-espect to the axis of the
telescope, but seems also to have provided for entire eliminatipi^ of
index error by making it possible to obser^•e all angles on opposite
sides of zero— a precaution possible in the later form only when
very small angles are measured. Rotation of the micrometer in
position angle is provided for as in the earlier form, but the in-
strument is not furnished with a position circle.
With one of these instruments of somewhat smaller dimensions TriflS-
(telescope 2J inches aperture and 3^ feet frtcus) Triosnecker made a Decker's
series of measurements at the observatory of Vienna which has nieasui^
been recently reduced by Dr Schur of Strasburg (^Kova Ada der caentB,
A'^;. Lcop. -Carol. Deulschen Akadanie dcr J^'uhirs/orschcr, xlv.
No. 3). The angle between the stars ( and g Ursae maj. (708""55)
was measured on four nights ; the probable error of a measure on one
night was ± 0"'44. Jupiter was mensurod on eleven nights in the
months of June and July 1794 ; from these measures Schur derives
the values S[i"'39 and 37""94 for the polar and equatorial diameter
respectively, at meaji distance, corresponding with ft compression
1/14"44. These agree satisfactorily with the corrcspondi'ig valuee
MICROMETERS.
JI I C Ft O i\i E T E R
35"-21, 3r"-60, 1/15-69 afternards obtained by Besscl (Komgsbcrgcr
Bcoba<IUunijm, xix. 102). From a series of measures of the angle
between japiter's satellites and the planet, made in June and July
1794 and in August and September 1795, Schur finds the mass
of Jupiter ■
a result which acconls perfectly with
1048-55±l-45
the received Talue of the mass derived from modern researches.
The probable errors for the measures of one night are ±0"-577,
±0"-8S9, ±0"-5i2, ±1"096, for Satellites I., 11., III., and IV.
resi>ectively. It is probable that Triesnecker deduced the index
error from his me.isures of the diameter of Jupiter, as, in 1794,
the measures of diameter are made on the same nights with those
of the measures of distance of the satellites, and it is possible that
measures of diameter i^y have been made in 1795 but not pub-
lished.
Consiilering the accuracy of these measures (an accuracy far sur-
passing that of any contemporary observations), it is somewhat sur-
prising that this form of micrometer was never systematically used
in any sustained or important astronomical researches, although a
number of instruments of the kind were made by DoUoud.
Probably the last example of its employment is an observation of
the transit of Mercury (November 4, 1868) by llr Mann, at the
Royal Observatory, Cape of Good Hope {MonlhUj KotUca li. A. S.,
vol. xxix. p. 197-209). The most iniijortant part, however, which
this tyi>o of instrument seems to have played in the history of
astronomy arises from the fact that one of them was in the posscs-
siou of Bcssel at Konigsberg during the time when his new obser-
Bes el's ^"'"'T ''"^re was being built. In 1812 Bessel measured with it the
ijboarva- '"S'^ between the components of the double star 61 Cygni and
.. " ' observed the great comet of 1811. He also observed the eclipse of
the sun on May 4, 1818. In the discussion of these observations
{K^nigshcrijcr BcolacJit., Abth. 5, p. iv) he found that the index
error of the scale changed systematically in diffej-eut position angles
by quantities which were independent of the direction of gravity
relative to the position angle under measurement, but which
depended solely on the direction of the measured position angle
relative to a fixed mdius of the object-glass. Bessel attributed this
to non-homogeneity in the object-glass, and determined with "^reat
care the ueccssar)- corrections. But he was so delighted with the
general performance of the instrameut, with the sharpness of the
images, and the possibilities which a kindred construction offered
for the nieasni-cment of considerable angles with micrometric
accui-acy, that he resolved, when he should have the choice of
a new telescope for the observatoiy, to secure some form of
heliouicter.
Nor is it dilhcult to imagine the probable course of reasoning
which led Besscl to select the model of his new heliometcr. Why,
he might ask, should he not select the simple form of Bollond's
first type f Given the achromatic object-glass, why should not it be
divided ' This construction would give all the advantage of the
j'ounger DoUond's object-glass micrometer and more than its sharp-
ness of definition, without liability to the systematic errors which
may be due to want of homogeneity of tiie objcct-gla.<!S ; for the lenses
will not bo turned with respect to each otlier,-but, in measurement,
will alw.iys have the same relation iu position angle to the line
joining the objects under observation. It is true that the scale will
require to be capable of being read with much gi-eater accuracy thon
luVntli of an inch — for that, even iu a telescope of 10 feet focus, would
corr.'spond with 2" of arc. But, after all, this is no practical diffi-
culty,— for screws can be used to sci'ai-atc the lenses, and, by these
screws, as in a Gascoignc micrometer, the sejmration of the lenses
can be measured ; or we can have scales for this purpose, read by
injfroscopcs, like the Trougliton' circles of Piazzi or I'ond, or those
of the Carey circle, with almost any required accuracy.
Whi ther Besscl communicated such a cotu^e of reasoning to
rsua- FraunhofKr, or whether that great artist arrived iwleiiendently at
■**'• like conclusions, we have been unablo to ascertain with certainty.
Die fact remains that before 1820' Frauuhofer had completed
one or more of the five heliometcrs (3 inches aperture and 39 inches
focus) which have since become historical instruments. In 1824
the great Konigsberg heliometcr was comineuccd, and it was com-
pleted in 1829.
To sum np briefly the history of the heliometcr. The first appli-
cation of the divided object-glass and the emi>loyment of double
iuiagei in astronomical measures is due to Savary iu 1743. To
Bon^jiior in 1743 is due the true conception of measuivment by
ilouldc image without the au.\iliary aid of a filar micrometer, vi;!.,
by changing (he distance between two object-glasses of equal focus.
To UoUi.nd in 1754 we owe the combination of Savary's idea of
the divided object-glass with Bouguer's method of measurement,
and the construction of the first nally practical hcliomcters. To
. Fraunhofer, sonic time wot long previous to 1S20, is ilue, so far as
He can ascertain, the constmction of the first heliometcr with an
,' ' Tlic elirlos by nvtcbculilcli, llien almoit cidusivcly uscj in Ccmiany, were
= Tile iU..nieiir ot Vemis win niootiircd »lih one of these lieliomcliM at the
•knnalon o( Ilrei!«u Ijy UranJo la 1S2U llirrlin Jalnltatli. UU, p. 104)
251
'.€., the first beliometer of tfaa
achromatic divided object*gIass,
modem type,
DoubU-Iniage Micrometers with Divided Lenses.
Various micrometers hav&been iurented besides the heliometer
for measuring by double image. Kamstlen's dioptric micrometer
consists of a divided lens placed in the conjugate focus of the inner-
most lens of the erecting eye-tube of a terrestrial telescope. The
inventor claimed that it would supersede the heliometer,- hut it ha«
never done anj'thing for astronomy. DoUond claims the independ-
ent invention and first constiuction of asimilar instrument (Pearson's
Pradical Astro^uyiny, vol. ii. p. 182). Of these and kindred instru-
ments only two types have proved of practical value. Aniici of
Modena [Mem. Soc. ItaL, xvii. (1815) pp. 344-359) describes a'
micrometer in which a negative lens is inti'oduced between the
eye-piece and the object-glass. This lens is divided and mounteil
like a heliometer object-glass ; the separation of the lenses produces
the required double image, and is measured by a screw. Dawes
has very successfully used this micrometer in conjunction with a
filar micrometer, and finds that the precision of the measures is
in this way greatly increased {Monihly Notices, vol. xviiL p. 58,
and Mem. R. A. S., vol. xxw. p. 147).
In the improved form ' of Airy's divided eye-glass micrometer
{Mem. R. A. S., vol. iv. pp. 199-209), the rays from the object'
glass pass successively through lenses as follows.
Lens
DlBtnnce from
next Lens.
Focal Les£tk.
a. Aq equtcoHT
e. Plar.o-convc
d. Piano-con vea
.
P
2
arbitrary =p
5
1
1
The lens b is diWded, and one of the segments is moved by a
micrometer screw. The magnifying power is varied by chaugiiig
the lens a for another in which p has a different value. The magni-
fying power of the eye-piece is that of a single lens of focus = |ji^.
In 1850 Vab pointed out that the other optical conditions could
be equally satisfied if the divided lens were made concave instead of
convex, with the advantage of giving a larger field of vie\y [Monthly
NoliecSt vol. x. p. 160).
The last improvement on this instrument is mentioned iu the
Report of the R. A. S. council, February 1865. It consists in the
introduction by Simms of a fifth lens, but no satiefactory descrip-
tion has ever appeared- There is only one practical published"*
investigation of Airy's micrometer that is woi-thy of mentioji,
viz., that of Kaiser {Annalai dcr Stennvarte in Leiden^ iii. pp.
111-274). The reader is referred to that paper for an exhaus-
tive history and discussion of the instrument.' It is somewhat
surprising that, after Kaiser's investigations, observers should con-
tinue, as many have done, to discuss their observations with this
instrument as if the screw-value were constant for all angles.
Stciulieil (Jounutl Sava}U de Munich, 2St\i February 1843) describes Stein-
a " hcliometre-oculaire*' which he made for the great Pulkowa re- heil's I
fi-actor, the result of consultations between himself aud the elder ocular
Struvc. It is essentially the same iu principle as Amici's micro- raicro-j
meter, except that the divided lens is an achromatic positive instead meterj
of a negative lens. Stmve (Description de I'ObscrDatoirc Central de
Pnlkowcty pp. 196, 197) adds a few remarks to Stcinheil's descrip-
tion, iu which he states that the images have not all desirable
Srecision, — a fault perhaps inevitable in all micrometers with
ividcil lenses, niid which is probably in this case aggravated by
the fact tliat tlie rays falling upou the divided lens have consider-
able convergence. He, however, successfully employed the instru-
ment iu measuring double stars, so close as 1" or 2", and using a
power of 300 diameters, with results that agreed satisfactorily
amongst themselves and with those obtained with the filar micro-
meter. If Struvc had emjiloyed a properly proportioned double
For dcsorii»tlon of ilic earliest fomi ««
■enteich OOseicatioUf. 1840.
iderstand tliat a very thoroiigli
Cambridge Pftil. Tram., vol. Ii.
111(1
Igarlon of Aii-j-'n doublc-inioge
micrometer used by Dr Copclaiid at .Mauiiiiua on Lord Lindsay's expedition has
U-cn made by him, and ^^ill soon be published.
* D.iwes OfoMt/ifj/ A'otifes. January 1808, aud ^/em. R. A. S., vol. xxxv. p. 150)
has su^gcstfd and used u valttablo iiuprorenient for producing round ImJKt\
instead of tlie eioncaicd imuKCs wUleti are otherwise inevitable when the rays
j-ass tlirougli a divided lens of which tlie optical centics are not in coincidence.
vi7., *' tlic Introduction of a diaphraj^ iiaving two circular apertuies toncliiiic
each other in a point coinciding with the line of eolllmatlon of the telescope, and
the diameter of each aperture exactly equal to the semidiumclcr of the cone cf
raya at the distiincc of the diaphragm from the focal point of the object -glnss."
Pnvetically the difficulty of making tliese diaphragms for the different powers of
the exact required eqnallty is Insuperable, bur. If the obsen-er Is content to lose
a eertnin amount of light, wc sec no re.ison why lliey mny not readily be made
sliphtly less. Dawes found the best metliod for the purpcse iu qutrstlon was to
limit the aperture of the obji-ct-glass by a diaphmgm having a double circular
flpeilurc. phielng the line Joining the centres of the circles approximately in the
position angle under meaauremeut, Duwes successfully employed the doublo
chcular aperture also with Amlcl's micrometer. Tlie present writer has succe«>-
fuUy used & simitar plan in mcasuiing position 3n;:les of aCentaurl with rh« helio-'
meter, viz.*, by placing circular diaphragms on the two segmcuts of the object-
■dass
252.
M;I-C R O M E T E K
[heijoiubtkb^
cjrcular ciftpnngm, fixed Bymmetrically with the axis of the telescope"
in froDt of *he divided lens and tuniij^ with the micronieter, it
is probable that .his. report on the instrument would hare been
«tiil more favoMable:^ This particulaj instnunent has historical
interest, having ' lell .Struve to some of those criticisms of the
Palkowa heliometer w£ich (jltimatelj bore such valuable fruit (see
below). ____
^EamsJen {Phil, Trans'/ voL lii, p, 419) has suggested the
division of the small speculum of a Cassegrain telescope and the
production of double image by micrometric rotation of the semi-
specula in the plane passiBg through their axis. Brewster {Ency.
jBrii., 8th ed., VoL liv. p. 749) proposes a plan on a like principle,
by dividing the plane mirror of a Newtonian telescope. A^in,
in an ocular heliometer by Steinheil double image is similarly
produced by a divided prism of total reflexion placed in parall^
rays. But practically uiese last three methods are failures. In
the last the field is full of false light, and it is not possible to give
eufficiently minute and steady separation to the images ; and there
are of necessity a collimator, two prisms of total reflexion, and a
small telescope through which the rays must pass ; consequently
there is great loss of light.
Micrometers Depending on Double Bxfractioit.
Biochoa'B^To'th'e^Abbe Kochon {Jour, de Pkys., liiL, 1801, pp. 169-198)
micro- is due the happy idea of applying the two images formed by double
meter refraction to tHe construction of a micrometer. He fell upon a
most ingenious plan of doubling the amount of double refraction of
a prism by using two prisms of rock-crystal, so cut out of the solid
as to give each the same quantity of double refraction, and yei to
double the quantity "in the effect produced. The combination so
■formed is known as Eochon's prian. Such a prism he placed
between the object-glass and eye-piece of a telescope. The separa-
tion of the images increases as the prism is aj^roached to the object-
glass, and diminishes as it is approached towards the eye-piece.
Ai^go {Compics Bendus, xxiv., 1847, pp. 40U-402) found that
in Eochon's micrometer, when the prism was approached close to
the eye-piece for the measurement of very small angl^ the
emallest imperfections in the crystal or its surfaces were incon-
veniently magnified. He therefore selected for any particular
measurement such a Eochon prism as when fixed betw-een the eye
and the eye-piece {i.e., where a sunshade is usually placed) would,
combined with the normal eye-piece employed, bring the images
about to be measured nearly in ' contact. He then altered the
magnifying power by sliding the field lens of the eye-piece (which
was fitted with a slipping tube for the purpose) aloEg tiie eye-tube,
till the images were brought into contact. By a scale attached to
the sliding tube the magnifying power of the eye-piece was deduced,
and this combined with the angle of the prism employed gave the
angle measured. \t p" is the refracting angle of the prism, and n
jthe magnifying power of the eye-piece; Sien jfjn will be the distance
(observed. Arago made many measures of the diameters of the
.planets with such a micrometer.
L Dollond {Phil. Trans., 1821, pp. 101-103) describes a double-
I image micrometer of his own invention in which a sphere of rock-
\ crystal is substituted for the eye-lens of an ordinary eye-piece. I j '
i^S instnunent ffiga. 31, 32) a k ftie sphere, placed in half-holes c u
OTCTCome by Dollond; and in the hands of Dawes {Mem. R. A. 8.]
Exzv. p. 144 sq.) such instnm[ient8 have done valuable eervice.^
They are liable to the objection that their employment is limited
to the measurement of very small angles, viz., IS" or 14" when tha
magnifying power is 100, and varying inversely as the power. Yet
the beautifaj images which these micrometers give permit the"
measurement of very diffirult objects as & check on measures mih
the parallel- wire micrometer.
7%e Modem Mdiometer.
The Konigsberg heliometer is represented in fig. 38. "So part of K6irig»
the equatorial mounting is shown in the figure, as it resembles in berg ^
every respect the usual Fratmhofer mounting. An adapter h is helio*
fixed on '
Rg- SL Fig. S2.
^ axis tt, BO thaT when its principal axis is parallel to the axis of
the telescone it gives only one image of the otject In a direction
parpen dictuar to that axis it must be so placed that when it is
moved by rotation of the axis hb the separation of the images shall
be parallel to that motion. The ancle of rotation is measured on
the graduated circle C. The angle between the objects measured
is — r sin 2^, where r is a constant to be determined for each mag- I
nifying power employed,* and e the angle through which the i
sphere has been turned from zero {i.e., from coincidence of its prin-
cipal axis with that of the telescope). 'The maximum separation
is consequently at 45* from zero. The measures can be made on j
both sides of zero for eliminating index error. Tbere are consider- ;
table difficulties of construction, bat these have been Bucceasfully '
VI DoDond pnnldea for chonflsg the power hj tlldlug tbo leu 4 nearer to or |
farther fron. r» *
tube, mSde of wood,
in Fraunhofer's nsmd
fashion. To this
adapter is attached a
fiat circular flange h.
The slides • earning
the segments of the
divided object-glass _. ^o
are mounted on a xig. sa.
plate, which is fltted and grotmd to rotate mnoothly on the fianga
A. Eotation is communicated by a pinion, turned by the handle
c (concealed in the figure), which works in teeth cut on the edga
of the flange h. The counterpoise %c balances the head about
its av^« of rotation. The slides are moved by the screws a and ft,'
the divided heads of which serve to measure the separation of the
segments. These screws are turned from the eye-end by bevelled
wheels and pinions, the latter connected with the handles o', h'.
The reading micrometers e, f also serve to measure, independently,
t^e separation of the segments, by scales attached to the slides;
snch measurements can be employed as a check on those made by
the screws. The measurement of position angles is provided for
\fj a graduated circle attached to the head. There is also a position
circle, attached at vi to the eye-end, provided with a slide to move
the eye-piece radially from "^e axis of the telescope, and with a
micrometer to measure the distance of an object irom that axis.
The ring which carries the supports of the handles o', h\ c if
capable of a certain amount of rotation- on the rube. The weight
of the handles and their supports is balanced by the counteipoi&e s.
This ring is necessary in order to allow the rods to follow the
micrometer heads when the position angle is changed. Complete
rotation of the head is obviously impossible because of the inter-
ference ctf the declination axis with the rods, and therefore, in some
angles, objects cannot be measured in two poEitions of the circle.
The object-glass has an aperture of 6| inches, and 102 inches foca-*
length.
There are three methods in which this heliometer can be used.
First Method. — One of the segments is fixed in the udrof th.
telescope, and the eye-piece is also placed in the axis. Measures
are made with the moving segment displaced alternately on oppo^te
sides of the fixed segment.
Second Method.— Out segment is fixed, and the measures are
made as in the first method, excepting thai the eye-piece is placed
symmetrically with respect to the images under meaanrement.
For this purpose the position angle of the eye-piece micrometer is
set to that of the head, and the eye-piece is displaced from the
axis of iht tube (in the direction of the movable segmenJ) by as
amount equal to half the angle under measurement
Third Method. — The eye-piece is fixed in the ^is, and. the
segments are symmetrically displaced from the axis each by a**
amount equal to half the angle measured.
Of these methods Bessel generally employed the first becanae of
its simplicity, notwithstanding that it involved a resettixj^ of the
right ascension and declination of the axis of the tube with each
reversal of the eegments. The chief obiections to the method are
that, as one star is in the axis c& the telescope and the other dis-
placed from it, the images are not both in focus of the eye-piece,'
and the rays from the two stars do not make the same angle with
the optical axis of each aegment Thus the two images under
measurement are not defined with equal sharpness and symmetry.
The second method is free from the objection of non -coincidence in
focus of the imagea, but is more troublesome in practice from t^s
necessity for frequent readjustment of the position of the eye-piece.
The third method is the most symmetrical of all, both in ohaer-
ration and reduction ; but it was not employed by Bessel, on the
gi-ound that it involved the determination of the errors of two
screws instead of one. On the other hand it is not neoeaaaiy to
reset the telescope after each reversal of the segment*.*
• ' Tlif aiitmncM of thr ortical ccaitref of tht ncpmentt (jont thr ey*-pi«je «rt tB
thU mot liod a« ] : sociint a[ the Knglf under moutiuTcmetiL Id Dowel'* boUoircter
ClilB would ■motinl to b dl&erencc of rifirtb of no IncL vlteo an an^lc of V It
nicasu'ed. For two dcfrtoeB ihc diOu cnct would nmoimt to nearlr ^^tb a' U
loch. Ue*»el cannncd his nteBBum to distnncc* coiuldermbly lc« then 1 .
* Is criticizing Bc««ul> clioin of mcUiuds and comirterlne the Id* of time
iSTolred Is each, II miui be ruaeoibcrcC ituii Fraunlioler provided nc aeaci ff
HEUOMBTEB.]
MICROMETER
253
When Bcssel ordered the Konigsberg heliotneter, he was anxious
to have the segmenta made to move in cylindrical slides, of which
the radius should be eoual to the focal length of the object-glass.
Fraunhofer, however, aid not execute ibis wish, on the ground
that the mechanical difficulties were too great
Wichmann states {Kimigsb. Bcobach., xxx. p. 4) that Bessel had
indicated, by notes in his handbooks, the following points which
should be kept in mind in the construction of future he lie meters :—
(1) The segments should move in cylindrical slides ;^ (2) the screw
should be proUcU,d from dust;* (3) the zero of the position circle
should not be so liable to change ;' (4) the distance of the optical
centres of the segments should not change in different position
angles or otherwise ; * (5) the points of the micrometer screws should
rest on ivory plates ; * (6) there should be an apparatus for changing
the screen."
The elder Struve, in describing the Pulkowa helicmieter,^ made
by Merz in 1839 on the model of Bessel's heliometer, submits the
following suggestions for its improvement ;* — (1) to give automatic-
ally to uie two segments simultaneous equal and opposite move-
ment;* and (2) to make the tube of brass instead of wood; toattach
the heliometer head firmly to this tube; to place the eye-piece pei-ma-
nently in the axis of the telescope ; and to fix a strong cradle on the
end of the declination axis, in which the tube, with the attached
head and eye-piece, could rotate on its axis.
Both suggestions are important. The first is originally the idea
of DoUona^(fig. 29) ; its advantages were overlooked by his son
(description of fig. 30), and it seems to have been quite forgotten
till rcsuggested by Stnive. But the method is not available if the
separation is to be measured by screws ; it is found, in that case,
that the dii'ection of the final motion of turning of the screw must
always be such as to produce motion of the segment against gravity,
otherwise the "loss of time" is apt to be variable. Thus the
simple connexion of the two screws by cog-wheels to give them
automatic opposite motion is not an available method unless the
separation oi the segments is independently measured by scales.
Struve*a second suggestion has been adopted in nearly all succeed-
ing heliometers. It permits complete rotation of the tube and
measurement of all angles in reversed positions of the circle ; the
handles that move the slides can be brought down to the eye-end,
inside the tube, and consequently piade to rotate with it ; and the
position circle may be placed at the end of the cradle next the eye-
end where it is convenient of access. Struve also points out that
by attaching a fine scale to the focussing slide of the eye-piece, and
knowing the coefficient of expansion of the brass tube, tne means
would be provided for detemuning the absolute change of the focal
length of the object-glass at any time by the simple process of
focusding on a double star. This, with a knowledge of the tempera-
ture of the screw or scale and its coefficient of expansion, would
enable the change of screw value to be determined at any instant.
Or, if we suppose the temperature of the instrument to be the
same in all its parts, the cnanged scale value becomes simply a
function of the reading of the focal scale.
^*J^ It is probable tliat the Bonn heliometer was in course of con-
""*^ struction before these suggestions of Struve were published or dis-
*6ter» cussed, since its construction resembles that of the Konigsberg and
Pulkowa instruments. Its dimensions are siiuilar to those of the
former instrument. Bessel, having been consulted by the cele-
brated statesman Sir Robert Peel, on behalf of the RadclifTe trus-
tees, as to what instrument, added to the RadclifFe Observatory,
reading the tcrews or eten the bcaJs rrom the eye-end. Bessel's practice was to
iincla.Tip in declination, lower and read off the head, and Uien restore the telc-
Bcope to Its former dccUoatlon rcadinff. the clocltwork meanwhile following the
stars In right ascension. The setting of both lenses sjumietricallT- would, under
such circumstances, be TCry tedious.
' Tliis most important Improvement would permit any two stars under measure-
ment each to be rlewed In the optical axis of eaih segment. The optical centres
of the segmenis would alw remain at the same distance from the eye piece at all
angles of separation. Thus, In measuiing the largest aa well as the smallest
aDRles, the Images of both stars would be equally B>'mmetrlcal and equally well
in focus. Modern (icliometera made with cylindiicul slides measure angles over
two degrees, the images remaining as sharp and perfect as wlien the smallest
angles are measured.
' Beaeel found, in (.ooise of time, that the original corrections for the errors of
his screw were no longer apj>licabtc. He ci.nsidei-ed that the changes were due to
wear, which would be much lessened if the screws were protected from dust,
• The tube, being of wood, was probably liable to warp and twist in a very
nncertaln way.
• We hsTo been unable to (hid any published druwing showbig how the seg-
ments are fitted In their ceUs.
5 We have been unable to ascertain the reasons which led Bessel to choose
frory planes for the end-bearing* ol his screws. He actxiallv Introduced them in
the KOnlgsberg heliometer in 1840. and they were renewed in 184S and 1850,
• A screen of wire gause, placed in front of the segment thronch which the
fainter star Is vie ned, was employed by Be&acl to tqualize the brilliancy of the
fmagca under obsers-ation. An ari-angement, aftciwards described, has been
fitted in modem heliometers for placing the screen In front of either segment by
a handle at the eye-end.
' This heliometer resembles Bessel's, except that its foot Is a solid block of
granite hi8U:ad of the ill-concelrcd wooden structure that supported his instrtl-
ment. The object-glass la of 7-4 Inches aperture and 123 inches focus.
• Detcription de f OHe>xatoii'« c. niral de Pultoiea, p. 206.
• Stelnheil applied such motion to a double-image micremeter mod© for StniTe.
This instrument suggested to StruTe the above-mentioned idea of employing a
almllar motion for the hdioir sicr. ■- * »
would probably most promote the advancement of astronomy,'
stiongly advised the selection of a heliometer. The order for toe
instrument was given to the Bepsolds in 1840, but *'variotis circum-
stances, for which the makers are not responsible, contributed to
delay, the completion of the instrument, which was not delivered
before the winter of 1848.*'" The building to receive it was com-
menced in March 1849 and completed in the end of the 'same year.
This splendid instrument has a superb object-glass of 74 inches
aperture and 126 inches focal length. The makers availed them-
selves of Bessel's suggestion to make the segments move in cylin-
drical slides, and of Struve's to have the head attached to a brass
tube ; the eye-piece is set permanently in the axis, and the whole
rotates in a cradle attached to the declination axis. They provided
a splendid, rigidly mounted, equatorial stand, fitted with every
luxury in the way of slow motion, and scales for measuring the
displacement of the segments were read by powerful micrometei*
from the eye-end.*^ It is somewhat curious that, though Struve'ft
second suggestion was adopted, his first was overlooked by the
makers. But it is still more curious that it was not afterwards carried
out, for the communication of automatic symmetrical motion to
both segments only involves a simple alteration previously de-
scribed. But, as it came from the hands of the makers in 1849, the
Oxford heliometer was incomparably the most powerful and perfect
instrument in the world for the highest order of micrometric
research. It so remained, unrivalled in every respect, till 1873; it
remains still, optically, the most powerful heliometer in the world;
and, with a few alterations, it might almost rival the most recent
instruments in practical convenience and accuracy. These altera-
tions, all of which could be made without great difficulty, are the
following : —
(a) Beyond the automatic symmetrical motion above- described,
the instrument should be fitted with means for adjusting the screeoa
from the eye-end (see footnote • in last column).
(6) The arrangement of the scales should be changed. At present
both scales are read separately by separate micrometers, each
relative to a separate fiducial L'ne. "What the observer requires is
the difference of the readings of the two scales, and this can obvi-
ously be most quickly and accurately obtained if the edges of the
two scales are brought together, and both axe read, relatively to
each other, by the same micrometer,
(c) The unsatisfactory motion in position angle should be replaced
by the action of a pinion (attached to the cradle) in the teeth of ft
wheel (attached to the tube)."
(d) The position circle should be read by telescopes or microscopes
attached to the cradle, and accessible from the eye-end.
(c) It would add greatly to the rapidity of work ard the ease of
the observer if a small declination circle were attached to the cross-
head, capable of being read from the eye-end.
As the transit of Venus of 1874 approached, preparations were
set on foot by the German Government in good time ; a commission
of the most celebrated astronomers was appointed, and it was re-
solved that the heliometer should be the instrument chiefly relied
on. The four long-neglected small heliometers made by Fraunhofer
were brought into requisition. Fundamental alterations were made
upon them: — their wooden tubes were replaced by tubes of metal;
means of measuring the focal point were provided ; s)*mmetrical
motion was given to the slides ; scales da each slide were provided
instead of screws for measuring the separation of the segments, and
both scales were read by the same micrometer microscope ; a
metallic thermometer was added to determine the temperature of
the scales. These small instruments have since done adrairabla
work in the hands of Schur, Hartwig, Kustner, and Elkio.
The Russian Government ordered three new heliometers (eacn of Ruaslai
4 inches aperture and 5 feet focal length) from the Repsolds, and the helio-
de&ign for^eirconstmclion was superintended by Struve, Auwers, mtterat
Fig. 34.
and Winnecke, the last-named making the necessary experiments at^
Carlsruhe. Fig. 34 represents the tj'pe of instnunent which re'
'.0 Manuel Juhnson, il.A., RadclJBe observer, Aitronomtail Ob$ervation* made
at the RadeUffe Observatory, Oxford, in the year 1&50, Introduction, p. lit.
H The illuminadon of these scales Is interesting as being the flr« application of
electricity to the Illumination of astronomical instruments Thin plntinum wh^
was rendered Incandescent by a voltaic current ; a small Swan light and condeaaec
would probably now be found more satisfactory.
13 This has been recently canled out by Stone, the prcKnt BadiPffe obtem^
00 GUI' I niggestlon
254
MICROMETER
l;UEUOilETEIt.
r.ora
Liud-
hnUo-
oieter.
salted from their labours. The brass tube, strengthened at the
beariDg points by strong truly-tmned cojlars, rotates in the cast-
iron cradle q attached to the declinatiou axis, a is the eye-piece
fixed in that ar b the micrometer for reading both scales.
Fig. 35.
e, d are telescopes for reading the position circle p^ e the handle
for quick motion in position angle, /the slow motion in position
angle, g the handle for changing the separation of the segments
by acting on the bevel-wheel ^ (fig. 35). A, is a milled head con-
nected by a rod with h' (fig. 35), for the
purpose of interposing at pleasure the
prism TT in the axis of the reading micro-
meter; this enables the observer to view
the graduations on the face of the metallic
thermometer tt (composed of a rod of brasa
and a rod of zinc), i is a milled head
connected with the wheel i'i' (fig. 35), and
afi'ords the means of placing the screen s
(fig. 34), counterpoised by w over either
half of the object-glass, k clamps the
telescope in declination, n clamps it in
right ascension, and the handles m and
I provide slow motion in declination and
right ascension respectively.
The details of the interior mecnanism
of the "head" will be almost evident
from fig. 35 without description. The.
screw, turned by the wheels at g\ acts in
a toothed arc, whence, as showu in the
figure, equal and opposite motion is com-
municated to tho slides by the jointed
rods V, V. The slides are kept firmly
down to their bearings by the rollers
r, r, r, r, attached to axes which are, in
the middle, vei-y strong spiings. Side-
shake is prevented by the screws and
pieces k, k, k, k. Th^ scales are at 7i, n ;
they are fastened only at the middle, and
arc kept down by the brass pieces t, t.
A similar heliometer was made by the
Repsolds to the order of Lord Lindsay c\
for his Mauritius expedition in 1874. It
dilfered only from the three Russian in-
struments in havin^j a mounting by the
Cookes in which tho declination circle
roads from tho eye-end.^ This instru-
ment was afterwards most generously
lent by Lord Lindsay to Gill for his ex-
pedition to Ascension in 1877.^
These four Rcpsold heliometers proved
to be excellent instruments, easy and
convenient in use, and yielding results
of very high accuracy in measuring dis-
tances. Their slow motion in position angle, however, was not all
that could bo desired. "When small movements were communi-
cated to the handle c (fig. 34) by tlie tangent screw/, acting on
a small toothed wheel clamped to the rod connected with the driv-
ing pinion, there wasiipt to be a toi-sion of the rod rather than an
immediate action. Thus the slow motion would take place by
jerks instead of with the necessary smoothm'sH and certainty.
When the heliometer part of Lord Lindsay's lieliomcter was ac-
quired by Gill iu ISTI*, he changed the manner of imparting tuo
motion in question. A square toothed racked wheel was applied to
the tube at r (tig, 34). Tliis wheel is acted on by a tangent screw
whose bearings are attaclied to the cradle ; the screw is turuL-d by
means of a handle supported by beaiings
attached to the cradle, and coming within
convenient reach of the observers liaud.
The tube turns smoothly in the i-acked wheel,
or cau be clamped to it at the will of the
observer. This alteration and the new equa-
torial mounting have been a-lmiiably made
by Grubb ; the result is con.;'letely success-
ful. The instrument so altereil has beeu
in constant use at the Cape Observatory
since Mai-ch 1S81 in determining the paral-
lax of the more interesting southern stars.
Still more recently the Repsolds have com- Yale
pleted a new heliometer for Yale College, CollM(»
New Haven, United States. The object-glass helio-
is of 6 inches aperture and 98 inches focal meter,
length. The mounting, the tube, objective-
cell, eHdes, i:c., are all of steel." The in-
strument is shown in fig. 36. The circles
for position angle and declination are read
by micrometer microscopes illuminated by
the lamp L; the scales are illuminated by
the lamp ?. T is part of the tube proper,
<ind turns with the head. The tube V, on the
contrary, is attached to the cradle, and merely forms a support for
the finder Q, the handles at/ and ^j, and the moving ring P. The
latter gives quick motion in position angle ; the handles at p
clamp and give slow motion in position angle, those at / cUmp
Fig. 36
and give slow motion in right a.sccnsiun and declination, n ift
the eye-piece, b tho handle for moving the segments, c the niicix)-
meter microscope for reading the scales and scnlo micrometer, d
the micrometer readers of tho position and declination circles, «
the handle for rotating tho large wheel E which carries the
screens. The hour circle is aUo roaJ by microscopes, and tho
instrument can be used In botli positions (tubo preceding and
' The primary object was to hare the olJJect-gla« mounted In «reel celU. which
more nearly concapond ta cxp.tmlon with claw. It became then tlcalr-iMc to
make the head of atocl for ^ako of uniliTiiil-.y ,<r maicilal, and the adTUllagu of
atcct In lightacu ouil rlgUltt) f*r iho tube th'rn bocamc evident.
w
aEUOMETEll.]
MICROMETER
255
following) for the elimmatlou of the effect of flexure on the position
Angles.
There 18 very little left to criticize in this instrument. It
inbraces the results of all knowledge and experience on the subject
to the present time. In one point, however, modern heliometers
bave a disadvantage compared with the older forms. A great
advance in accuracy was, no doubt, made when the screw was
abandoned as a means both of moving and measuring the displace-
ment of the slides.^ But it is obviously much quicker to read and
record the indication of one screw-head than to bisect two or four
scale-divisions and enter the corresponding readings. Auwers, in
his researches on the parallax of 61- Cygni,* was able, with
the Konigsberg heliometer, to make forty pointings in about an
hour ; it is quick work to make sixteen pointings (reading two
divisions on each scale at each pointing) with the modern heliometer
in the same time, when attention is paid to the desirable reversals
of the segments and of the position circle and the resettings in right
ascension and declination. 'Now time during opportunities of good
definition (or otherwise)' is too precious to be sacrificed, if it can be
saved even by ten-fold labour afterwards. Carrington * has suggested
the possible use of photography to record the readings of astro-
nomical circles, and since his day "Swan lights" and "sensitive
dry plates" seems to have brought his suggestion within the range
of practice. A special microscope, fitted with an aplanatic photo-
graphic objective and a well-contrived carrier, might be made
automatically to expose a different part of a narrow dry plate, by
mere pressure or turning of a button after each bisection. Each
plate might easily record the sixteen bisections which constitute a
complete measure of two pairs of stars (as in a parallax determina-
tion). As it is only necessary to photograph two divisions of each
scale, the photographic enlargement of these divisions need only be
limited by the sensitiveness of the plates and the power of the
illumination to produce a picture in a conveniently short space
of time. The plates employed at night could be conveniently
developed the following day and measured with a special apparatus
at any convenient time and with almost any desired accuracy.
Were such a system reduced to pl^ctice it would at least double,
perhaps treble, an observer's possible output of work
1 Gill has introduced a powerful auxiliary to the accuracy of helio-
'jm ^^ *netcr measures in the shape of a reversing prism placed in front
of the eye-piece, between the Intter and the observer's eye. If
measures are made by placing the image of a star in the centre
of the disk of a planet, the observer may have a tendency to do so
systematically in error from some acquired habit or from natural
astigmatism of the eye. But by rotating the prism 90" the image
is presented entirely reversed to the eye, so that in the mean of
measures made in two such positions personal error is eliminated.
Similarly the prism may be used for the study and elimination of
personal errors depending on the angle made by a
double star with the vertical. The best plan of
mounting such a prism has been found to be the
following. V, P (fig. 37) «re the eye lens and field lens
respectively of a ilerz positive eye-piece. In this
construction the lenses are much closer together and
the diaphragm for the eye is much farther from
the lenses than in Ramsden's eye-piece. The prism Fig-' 37.
p ii fitted accurately into brass slides (care lias to be taken in
the construction to place the prism so that an object in the
centre of the field will so remaiu when the eye-piece is rotated in
its adapter). There is a collar, -clamped by the screw at S, which
is so aajusted that thu eye-piece is in focus when pushed home, in
its ada'pter, to this collar. The prism and eye-piece are then
rotated togetlier in the adapter.
Oa the theory of the heliometer and Its n«o consult Bessei, Asironomische
Vnlersuchungen, vol.i.', Hansen, AusfiihrJiche Methode mit iJem Frattnhoferschen
Eelionieler anzjistellen, Gotlm, 1827 : Cliauvenet, Spherical arid Practical Astro-
nomt/, ToL 11. pp. 403-436, Philadelphia and London, 1876; SeeliRer. Theorie
det Ileliomeiers, Leipslc, 1877 ; Lindsay and GUI, Dunecht PubUcaticn:, vol. il.,
Dunecht(for private dixulatlon), 1877; Gill, Mcmoirt of the Royat Astronomical
Socielv, vol. xlvl. pp. 1-172
IficromeUrs which Involve the Employment of the Diurnal Motion.
Advantage is often taken of the diurnal motion to measure the
relative positions of stars. The varieties of reticules and scales that
have been employed are far too numerous even for mention in
detail. The following are the means and methods by which most
work has been done, and they are typical of all the others. In the
focus of his meridian telescope Lacaille had a brass diaphragm in
I discussion of Bosel's observations ("FnraUux<
Cyjfnl," Atf/iandlungm der Konigl. Alcad. rfer yVistenicha/(en ru'Serhn, 1868) he
iliown, are apt to wear and ehanpe their errors. It is, besides, unde^liable to opply
force and frlcilon to a delicate standard of measure
* MMiron. A'acfiyichten. No. 1418.
■ For example. In determining the diurnal pnrallait of a planet the most
favourable conditions are limited on the one hand by the uncertaintleg of refrac-
tion at large zenith distances, and on the other by the snwll parallax factors of
email zenith distimces. It \vould probably be best to secure all the observations
notild only be possible with special faciUtiesfor
between fiO° and 60' ZD, and tli
reading the scales.
* ifonthii, Jfcticci R. A. S.
X. p. 46.
which wag cut a hole, havinc parallel, sharp, straight edges of the La-
shape shown in fig. 38. f he longer diagonal of the rhomboid caille'
so termed was at right angles, and tiie shorter parallel, to the rhom-
diurnal motion. The method of observation consisted in noting boid.
the instant of ingress and egress of encli star which pi-esentcd itsell".
The mean of the times thus noted for eacli star gave the time of its
transit over the imaginary line ab, whilst the diirprenco brtwcea
the instant of ingress and that of
egress (converted into arc by the
known approximate declination) gave
the length of the chord traversed by
the star parallel to the imaginary
line cd. Hence (the dimensions of
the rhomboid beingknown)thediffer- c-
ence of the star's declination from
the line cd became known (the ob-
server was of course careful to note
whether the star passed to north or
south of cd). Thus every star that
crossed the field was observed, all
their ri§ht ascensions were referred
to the clock-time of passing ab, and
all their declinations to that of cd ; hence their mutual diffw-
ences of right ascension and declination were known. In this
way, in the short space of ten months, Lacaille observed nearly tea
thousand stars at the Cape of Good Hope in the years 1751-52.*
Fraunhofer's ring micrometer consists of a ring of steel, very truly Riug.i^*
turned, mounted in a hole cut in a circular disk of glass. The ring is cromet' >
placed in the foous of a telescope, and viewed by a positive eye-piece.
The observer notes the instants when the two objects enter and
emerge from each side of the ring. The only data rec^uired for com-
puting the difference of right ascension and declination of the two
objects arc the times above mentioned, the diameter of the ring,
and the approximate declination of one of the objects. The latter
is always known. The methods of determining the former and of
r«ilucing the observations are to be found in every work on practical
astronomy. The ring micrometer has been largely used in observ-
ing comets.
Argelander, in mal.ing his famous survey of the northern heavens,* Arge-
employed a semicitcle of glass, the straight edge of which (truly laade/
ground) crosses the centre of tlie field of view at right angles to the scale,
diurnal motion of the stars. Differences of right ascension wore
directly observed at this edge, whilst differences of declination were
noted by strong dark lines drawn at right angles to the edge at eacli
10' of arc. A telescope of 3 inches aperture with a magnifying power
of 10 diameters commanded a field of Z" 20' in declination. One
observer was placed at the telescope, another at the clock. The
telescope observer marked the instant when the star touched the
glass edge, by calling sharply the word "eight" or "nine," &c.,
which also indicated the magnitude; the same observer also noted
and recorded the reading of the declination scale (where the star
crossed it), without removing his eye from the telescope. The
clock observer wrote down the magnitude called out by the telescope
observer, and the instant by the clock when the word was given.
The two records were then compared after the observations of the
night were over. In this way Schbnfeld and Kruegcr (Argelander's
assistants) observed and catalogued about three hundred thousand
stars. The probable error of an observation is ^bout ±0*7 sec. in
right ascension and ±0'"4 in declination.
Bond' employed a very similar arrangement, differing only from Bond's
Argolapder's in having the scale cut on a sheet of transparent mica mica
-iVTTffth of an inch in thickness. Very oblique illumination was decline
employed, and the divisions and figures were seen bright upon a meter,
dark background. The range of declination was limited to 10',
the scale was divided to 10", the right ascensions were observed by
chronographic registration, and the great refractor of the Cambridge
U. S. Observatory (with an aperture of 15 inches and power of 140)
was employed. The probable errors in right ascension and declina-
tion were found to be ±0*06 sec. in right ascension and ±0""6 in
declination — results of marvellous accuracy considering the amount.
of work accomplished in a short time and the faintness (eleven to
twelve magnitudes) of the stars observed,
"VVe were on the point of criticizing Bonds programme as some- Peters'*
what too ambitious for realization without cooperation (it would zones,
take about twenty-six thousand hours of observing to carry out the
scheme for the northern hemisphere alone) when we received from
Peters of Clinton, U. S., the first twenty maps of a series which will
include the whole of the sky between declination + SO'* and - 30°. If
we consider that all the stars in these maps of the eleventh magni-
tude or brighter have been observed by a method similar to Bond's,
that the enormous additional labour of frequent revision has beea
undertaken, and all stars visible with a power of 80 in a telescope of
13 inches aperture (about fourteenth magnitude) have been filled in
tf Lacaille, Calum Australe SteUifemm, Pails, 1763, and A Catalogue q/' 9765.
Stars, from the Obtercations of Lacaille, London, 18-;7,
^ AHa$ dei Nordlif^ef
256
M I-C — M I C
fy ali''nTnrtit, linA Ihni all this results from Ihc lOinuM Inlnar of a
Isinglclbscncr, wo find tliat our ideas of We jmsvllc liavc to Uo modi- j
lied, when sueli a imui imdertakes a work with pcrsihlciit unity of
purimsc for more than twenty years (!860-63>.
Berlin ' TluTe is an ingenious mode of rcnisterin^'iliU'eroncos of declination |
dedino- ;that lias liceii in use at the Berlin Ohscrvntory since 1S79, an.I is
»rai*- iScscribid by Dr Knarrc in tW) ZciiS'-hrifl fiir IiislnuncnUnhiinih '
for July ISSl. The iustrumcnt is called a declinograph. It has a J
web moved in declination by a quick-acting screw ; the same screw ,
carries a travelling pricker or j.oint. The observer having bisected |
a star by the wire has simply to coinjiross an india-rubber ball con-
nected by a flexible tube with a thin metal box made on the prin-
ciple of the vacuum chamber of an aneroid barouieter. The ex-
pansion of tliis box so proiluccd brings a sheet of pajwr in contact
with two prickers, one the movable pricker before mentioned, the
other a fixed pricker. Tlio action of the va-uuni box also
automatically shifts the paper (a long roll) by a small quantity at
each observation, so that successive observations are ri-corilcd in
regular order. To obtain the observed differences of declination it
is tlien only necessary to measure with a glass scalo (divided for
the special telescope to 10") the distance of each record of the
noving pricker from the fixed pricker. It is found, with this
declinograph on the Berlin equatorial, that the observed declina-
tions have only a probable error of ±0"'9. It is obvious that by
using a dironograph in conjtinction with this instrument both
right ascensions and declinations conUl be recorded with great
accuracy and rapidity.
MisaUancous Micrometers,
VSx^Aj Clausen in 1841 {Ast. Nach., No. 414) proposed a form of micro-
glass meter consisting of a divided plate of parallel glass placed witliin
micro- , the cone of rays from the object-glass at riglit angles to the
meter. ' telescope axis. One half of this plane remains fixed, the other
half is movable. When the inclination of the movable half with
respect to the axis of the telescope is changed by rotation about an
axis at right angles to the plane of division, two images are pro-
duced. The amount of separation is veiy small, and depends on
the thickness of the glass, the index of refraction, and the focal
length of the telescope. Secchi (Conijitts Ucmlt'S, xli., 1S55, p.
900) gives an account of sonie experiments with a similar micro-
raetcr ; and Porro (.ComptcsKtiutiis, xli. p. 1053) claims the original
invention and construction of such a micrometer in 1842. Clausen,
however, has undoubted prioiitj'. Helmholtz in his " Ophthalmo-
meter" has employed Clausen's principle, but arranges the plates
so that both move symmetrically in opposite directions whh resjiect
to the telescope axis. Should Clausen's micrometer be employed
as an astronomical instrument it would be well to adopt the im-
^provement of Helniholtz.
Qhost Bui tonttnd Grubb (Monthly Kotiees, toI. xli. p. 59), after calling
iuicro- attention to Lament's paper (Jcihrbuch dcr IC. S. b, Miiuchrjt/\y,
meter. 187) and Littrow's paper ( /'yoc. of Vienna. Acnd. of Sciences, vol. xx.
p. 253) oA a like sul»ject, jiroceed totlescribe a most ingenious form
of " Ghost Micrometer," in which the iinnr/e of a fine line or lines
ruled in (or rather cut through) a silver film deposited on glass is
'formed at the conmion focus of an object-glass and eye-piece of a
telescope. A faint light being thrown on the outside of the silvered
f)latc, there appear bright lines in the field of view. AVe have not
lad an opportunity of testing this, nor Crubb's more recent
models ; but, should it be foutul possible to produce such images
satisfactorily, without distortion and with an apparatus convenient
and ligid in form, such micrometers will probably supersede the
filar micrometer. Their absolute freedom from diffraction, the
perfect control of the illuniiuation and lliirkuess of the lines, and
the accuracy with which it will be possible to construct scales
for Eone observations will, be. important features of the new
.method.
For the use of micrometers in connexion with the microscojic,
pee p. 277 of the present volume (D. GI.)
MICRONESI.\. ' Tlie term " Micronesia '" embraces I
tliat region of tlie Pacific nortli- of tlie great >[elanesian |
islands, where, eitlier iicrhaps from a greater or more raiud
subsidence, or from the decreasing activity northwards of :
■tbe coral bitildeis, the islands become, generally speaking,
smaller and fewer, and finally cea.se. Accordingly, except-
ing the Marianas or Ladroncs, which are of volcanic
origin, and a few isolated instances of elevation in tlie '
Carolines, the Microncsian islands, though many of the !
group.s cover a vast area, are almost without exception verj"
small low coral (atoll) formations. Besides the LxPitoxE
apd CxroLiXE 1sl.\N"DS (7.1.) Micronesia includes the J
Marshall and Gilbert groups, and some geographers '
include the Anson group, fa uuinber of small widely- ,
scattered i6lef3 to the west of Hawaii, the Magellan
group farther west, .and tbe Benin 'Islands north of the
Ladroncs.'
North-easterly ■ninds prevail during the winter months
over the Marshalls, Ladrones, and Carolines, except in
the extreme west, while between May and .September the
influence of the monsoon causes unsettled weatlier from
the west, with heavy gales. In the Gilberts the south-east
trade-wind brings fine weather at this season.
The ethnological features of Micronesia are much more
definite than the geographical, for its populations form
one great branch of the fair Polynesian race, distinguished
from the other by weB-marked differences in appearance,
language, and institution.?. Its ethnological relations are
not thoroughly understood. The proximity of Jajian and
the Philijipines on the west and of the Papuan and South
Polynesian islands on the south and south-east suggests,
what in fact we find, a combination of elements in different
degrees of fusion. In some places the oblique Mongolian
eye is noticed, and (along with certain Indo-Chinese
custoiuji) there is often a scantiness of beard and general
"Malay" look which increases westwards, and seems to
imply relations with the archipelago subsequent to the
departure tlience of the pure Polynesians. In the Gilberts
the traces of Polynesian (Samoan) influences are evident,
and are confirmed by tradition. Among the Carolines and
the Marshalls darker and more savage communities arc
found, suggesting a Melanesian clement, which is further
traceable in the Kbon (Marshall) and other languages.
Each of the. four groups, from long isolation, has devel-
oped peculiarities of its own. The most advanced were
the "Chamorros" of the Ladrones, owing to the greater
natural resources of the islands, and iierhaps more frequent
contact with influences from the west ; but as a separate
peo|ile they no longer exi.st, having been nearly extermin-
ated by the Spaniards in the ITth century. Kext in
advancement come the Carolines. The general type is a
well-proportioned rather slightly built figure, with small
and regular features ; head high and well-proportioned,
but forehead rather retreating, and narrow at the temples ;
cheek bones and chin slightly prominent ; colour somewhat
darker than the Polynesians, the Marshalls being darker
and more vigorous than the Carolines, while the Gilbert
type is still darker and coarser. The upper class greatly
surpasses the common people in physique and intelligence.
There is a peculiar division of .society into septs or
clans, the membership of which constitutes the closest tie.
Per.-rons of the satne .sept must not intermarry, and when
two islands or communities meet in war the members of
one scjit, however widely separated by distance of space
or time, will not injure or fight with each otiier. Eac'
community is usually composed (but there are local differ
cnces) of — (1) an upper class of chiefs, from among whom
the head {tnmol or irof) is chosen ; (i) a lower but still
noble class ; and (•'3) common people, nlbstly without
rights of property. These last are only allowed one wifa.
Assemblies of the chiefs cverj-wherc limit the kingly
nutliority. In the Mar.--halls the sovereign has lost his
control over many of the atolls, and in Ihc Gilberts the
above diatinctions have nearly disappeared : the licadslyp
has lajiscd, and. especially in the southern islands, the man
of largest sub.-tance is the most powerful, and somelinic,'*
e-!tabli»hcs a local supremacy. Here and there are frace^i,
as in Tonga, of a spiritual sovereign, the descendants
probably of a conquered dynasty. • Succession is through
the female side, which assures to women a certain position,*
' TI:>-0 i«landv. \\hh\\ contain a nii.vod inimij:vanl population, are
claiinc.f and have U-rn recently survoye.l, by .lapan. Bui lliry were
annexed to En^-laml l.y Captain Ueochey iu IS'.'?. (S»« Vou Kitllili,
Di uk n M-iUi/Uiltii cin'crRciM naeh . «. . J/ifl-roiiejifii. tc, vol. ii.)
M I C — M I C
257
and leads besides to some curious results (see paper by
Kubary in Das Ausland^ 1880, No. 27). The upper class
are the keepers of traditions, boatrbuilders, leaders of
expeditions ; tattooing is generally done by them, the
amount increasing with a man's rank j the custom here
still has definite religious associations. Both sexes are
tattooed. The people are singularly amiable and well
disposed, but will repay ill usage with treachery. The
women (although chastity is not expected before marriage)
are somewhat more moral than the Polynesians, and are
treated with respect, as are the a^ed. The natives are
polite and hospitable to strangers (except on the poorer and
ruder islands), bright and intelligent, active traders, expert
cultivators and fishermen. They have a hand-loom from
which beautiful fabrics of banana, hibiscus, and other fibres
are produced. The Marshall Islanders are the boldest
and most skilful navigators in the Pacific. Their voyages
of many months* duration, in great canoes sailing with
outrigger to windward, well-provisioned, and depending on
the skies for fresh water, help to show how the Pacific
was colonized. They have a sort of chart, medo^ of small
sticks tied together, representing the positions of islands
and the directions of the winds and currents. A two-edged
-weapon, of which the blade is of sharks* teeth, and a
defensive armour of braided sennit, are also peculiar to the
islands ; a large adze, made of the Tridacna gigaSj was
formerly used in the Carolines, probably by the old
Guilder race.
Tlio languages of Micronesia, though grammatically alike, differ
widely in theii- vocabularies. They have the chief characteristics
of the Polynesian, with Malay affinities, and peculiarities such as the
use of suffixes and inseparable pronouns and, as in Taffal, of thein6x
to denote changes in the verb ; in the west groups there is a tend-
ency to closet! syllables and double consonants, and a use of the pala-
tals c7i, ^', jA, the dental tk, and s (the last perhaps only in foreign
words), which is alien to the Polynesian. These letters are
wanting in the Gilbert language, which differs considerably from
all the others, and has much greater affinities with the Polynesian.
The religious myths are generally identifiable with the Polynesian,
but a belief in the gods proper is overshadowed by a general
deification of ancestors, who are supposed from time to time to
occupy certain blocks of stone, set up near the family dwelling, and
surrounded by circles of smaller ones. These stones are anointed
with oil, and worshipped with prayer and offerings, and are also used
for purposes of divination, in which, and in various omens, there is
a general belief. In the ilarslialls, in place of these stones, certain
palm trees are similarly enclosed. The spirits also sometimes
inhabit certain birds or fishes, which are then tabu^ as food, to tho
family ; but they will help to catch them for others. All this
closely recalls the .karwars or ancestral images of New Guinea.
Temples are very rare, though those blocks of coral are sometimes
surrounded by a roofless enclosure opening to the west. The bodies
of tho dead, and sometimes even of the sick, are despatched to sea
westwards, with certain rites ; those of the chiefs, however, are
buried, for the order has something essentially divine about it;
th«ir bodies tlierefore are sacred, and their spirits naturally assume
tho position above described. Such a belief greatly strengtheus the
king's authority, for the spirits of his ancestore are necessarily more
powerful than any other spirits. Thus too it comes that the chiefs,
and all belonging to them, are tabu as regards the common people.
There are various other subjects and occasions of tabu, but the
institution has not the oppressive and all-pervading character
which it has in Polynesia. Its action is often economical or
charitable, e.g. , the ripening cocoa-nuts are tabu as long as the bread-
fruit lasts, thus securing the former for future use ; or it is put on
after a death, and the nuts thus saved are given to the family—
a kindness to them, and a mark of respect for the dead.
The flora of the Gilbert and JIarsnall groups is of the usual
oceanic character, with close Indo-Malay affinities. It is much
poorer than that of the Carolines,^ with its Moluccan and Philip-
mne elements, and this again is surpassed by that of the Ladrones.
In the Gilberts the scattered woods of cocoa-palm and Pandamcs
have little undergrowth, while the south Marshalls, being within the
^belt of constant precipitation, have a dense growtli of (mostly) low
trees and shrubs, with here and there a tropical luxuriance and
variety unusual oh atolls. The Paiidanus grows wild profusely, and
is of exceptional importance, being the chief staple of food, so that
^ About 180 species have been observed on Kusaie, one-fourth of
all the plants being ferns. '^
the cocoa-nut, which, however, flourishes chiefly in the Gilberts, is
used mainly to produce oil for exportation. The bread-fruit gi-ow*
chiefly in the south Marshalls. The taro (Antm cordi/olium
and others) is cultivated laboriously, deep trenches being cut in
the solid rock for its irrigation, but; this and other plants of cultiva-
tion, and indeed the vegetation generally, fall off in number and
quality northwards. Various vegetables are grown on soil im-
ported for the purpose. Marine plants are rare. Wilkes found oa
Makin Island, Gilbert group, a " fruit resembling the gooseberry,".
called '*teiparu,"from wliich a preserve is made. This seems very
like the tipari or Cape gooseberry of India {Pkysalis pcrumaTia).
And their Icaraka, a drink made from the sap of the flower-stalk of
the cocoa-palm (unfermented before the arrival of Europeans), recalb
the arrack of southern Asia.
The fauna, like the flora, becomes poorer eastwards, birds being
much more numerous on the high islands than on the atolls, where
the few are chiefly aquatic. On Bonabe (Puynipet) out of twenty-
nine species eleven are sea birds, and of the remaining eighteen seven
are peculiar to the island. From the Pelews fifty-six species are
recorded ( twelve peculiar), and from the neighbouring Mackenzie
group (Ulithi) twenty (six peculiar). Yet curiously no species is
recdrded common to these two groups and peculiar to them. The
common fowl is found everywhere, wild or tame, and in some places
is kept for its feathers only. The rat and a Pteropus are the only
indigenous land mammals. The Indian crocodile is found as far
east as the Pelews. There are five or six li:^ards, including a
Occko and Ablephorus. Insects are numerous, but of few kinds.
Scorpions and centipedes are common, but are said to be harmless.
The houses in the Gilberts and Marshalls (much less elaborate
than in the Carolines) consist merely of a thatched roof resting on
fiosts or on blocks of coral about 3 feet high, with a floor at that
evel, which is reached from an opening in the centre. On this
the principal people sleep, and it serves as a storehouse in-
accessible to rats, which infest all the islands.
The Marshall archipelago consists of two nearly parallel chains
of atolls, from 100 to 300 miles apart, the west known as Eahk, the
east as Ratak, They lie between 4° 30' and 12° N., and between
165° 15' and 172° 15' E., and run about N.N.AV. and S.S.E.
They were discovered in 1529 bySaavedra, who, observing the fine
tattooing of the inhabitants (the first allusion to the practice in
the Pacific), called them Los Pintados. Among modern voyagers
"WaUis first visited them in 1767 ; Captains Marshall and Gil-
bert reached them in 1788, and Kotzebue (1816) explored them
more thoroughly. Each gi'oup contains fifteen or sixteen atolla,
which range from 2 to 60 miles in circumference. An anomalous
feature is reported on some of them, viz., that the greater pro-
portion of land, or at all events of soil, is not found as usual on the
windward side of the lagoon, for the prevailing north-east wind
sweeps, it is said, the materials of which the soil of such islands is
composed across to the lee side. Jaluit Island is the commercial
emporium of the whole region. There is a curious tradition on
Ebon Island of the Darwinian fact that the atoll once formed the
barrier reef of an island now sunk beneath the lagoon. Thepopula-
rion of Ratak is about 6000, of Ealik 4000 ; there is little intercoui"se
between the two groups.
The Gilbert archipelago, discovered by Byron in 1765, is
geographically a south continuation of the Marshalls, the channel
separating them being 60 leagues wide. It lies between 2° 40'
S. and 8" 20' K, and between 172° 30' and 177° 15' E., and con-
tains sixteen atolls, not including two hiUy islands, Banaba and
Nawodo, which lie 5' to 6° to the west. Several have good anchorages
inside the lagoon, with entrances on the lee side. On some the lee
or west reef is wanting, owing to the abrading force of the west
storms. During these large trees are washed ashore, their roots
containing pieces of fine basalt, of which implements ore made.
There is a lar larger proportion of land to submerged reef and
lagoon than in the Marshalls, the land sometimes nsing 20 feet
above the sea, whereas in the Marshalls the average level of the
reef rock is less than a foot above the surface^ but, though the
supply of fresh water is exceptionally great, in fact enough for the
luxury of a bath, the soil (especially in the south) is very mueli less
Sroductive. Yet the population, about 50,000, is exceptionally
ense. The usual scattered houses are replaced by compact rows
of roofs which, shaded by cocoa-palm, and each with its boat-shed
below, line the shore. 'Their numbers are unchecked either by the
constant practice of abortion or by fighting, to which they are
much addicted, their weapons being more formidable than those
of their neigliboura. This exceptional vigour may be due to the'
decidedly hybrid character of tlie race. Hawaiian missionaries,'
under American superintendence, have laboured here since 1857.
See also Findlay's Sailing Directtont for the North Pacific ; Roper's KorfU
Pacific Pilol and Nautical *l/o?o:t"H<, vols. Jtxxi. and ixxv. Other authorItI«i
are Gerlnnd In Waitz't Aathropoloyie der KaturvStker. vol. v.: Jlcinlcke. />/«
Intein dts S(iilen Oceans; Hole'n Elhnography and Philology of Wilkes'a U. Sj
Explorini) Erpeditioni-Kotzchm and ChamXaso. Enldectvnffsreiie in die Sudtet;
Proc. Z^ol. Soc, 1872 and 1877. v(C. T.)/
MICROPHONE. _ See Telepho>-e.
25»
MICROSCOPE
THE ' microscope is an optical instrmnent for the ex-
amination of minute objects or parts of objects,
which enlarges the visual pictures formed upon the retina
of the observer by the rays proceeding from them.
Microscopes are distinguished as simple or compound.
In the former, the rays which enter the eye of the observer
come from an object brought near to it after refraction
through either a single lens or a combination of lenses
acting as a single lens, — its action as a "magnifier " depend-
ing on its enabling the eye to form a distinct image of the
object at a much shorter distance than would otherwise be
possible. The latter consists of at least two lenses, so placed
relatively to the object, to the eye, and to one ahother that
an enlarged image of the object, formed by the lens placed
nearest to it (the " object-glass "), is looked at through the
lens nearest the eye (the " eye-glass "), which acts as a
simple microscope in "magnifying" it; so that the com-
pound microscope may be described as a simple microscope
\ised to look at an enlarged image of the object, instead
of at the object itself.
History of the Simple Microscope. — Any solid or liquid
transparent medium of lenticular form, having either one
convex and one flat surface or two convex surfaces whose
axes are coincident, may serve as a " magnifier," — what is
essential being that it ^all have the power of so refract-
ing the rays which pass through it as to cause widely
diverging rays to become cither parallel or but slightly
divergent. Thus if a minute object be placed on a slip of
glass, and a single drop of water be carefully placed upon
it, the drop will act as a magnifier in virtue of the con-
vexity of its upper surface ; so that when the eye is
brought sufficiently near it (the glass being of course held
horizontally, so as not to distort the spherical curvature of
the drop) the object will be seen much enlarged. And if
a small hole be made in a thin plate of metal, and a
minute drop of water be inserted in it, this di-op, having
two convex surfaces, will serve as a still more powerful
magnifier. There is reason to believe that the magnify-
ing power of transjjarent media with convex surfaces was
very early known. A convex lens of rock-crystal was
found by Layard among the ruins of the palace of Nimrud.
And it is jiretty certain that, after the invention of glass,
hollow spheres blown of that material and filled with
water were commonly used as magnifiers (conip. vol. xiv.
p. 577). The perfection of gem-cutting shown in ancient
gems, especially in those of very minute size, could not
have been attained without the use of such aids to the
visual power; and there can be little doubt that the
artificers who could execute these wonderful works could
also shape and polish the magnifiers best suited for their
own or others' use. Though it is impossible to say when
convex lenses of glass were first made by grinding, it is
quite certain that they were first generally used to assist
ordinary vision as " spectacles," the use of which can be
traced back nearly six centuries ; and not only were
spectacle-makers the first to produce glass magnifiers (or
simple microscopes), but by them also the telescope and tne
compound microscope were first invented. There seems
no reason to believe, however, that lenses of very high
magnifying power (or short focus) were produced until
a demand for them had been created by the introduction
of the compound microscope, in which such lenses are
required as " object-glasses "; and the difficulty of working
lenses of high curvature with the requisite accuracy led in
the first instance to the employment of globules made by
fusing the ends of threads of spun glass. It was in tk-s
way that Robert Hooke shaped the minutest of the lenses
with which he made many of the numerous discoveries
recorded in his Microgrnphia; and the same method was
employed by the Italian microscopist Father Di Torre. It
seems to have been Leeuwenhoek that first succeeded in
grinding and polishing lenses of such short focus and
perfect figure as to render the simple microscope a better
instrument for most purposes than any compound micro-
scope then constructed, — its inferiority in magnifying power
being more than counterbalanced by the superior clearness
of the retinal picture. And, in despair of any such modi-
fication in the compound form as should remove the optical
defects which seemed inherent in its plan of construction,
scientific opticians and microscopic observers alike gave
their chief attention for a considerable period to the
improvement of the simple microscope. In order that the
nature of these improvements may be understood, the
principle of its action must be first explained.
The normal human eye has a considerable power of self-
adjustment, by which its focal length is so varied that it
forms equally distinct pictures of objects brought within
ordinary reading distance (say 10 inches) and of objects
whose distance is many times that length, — the size of the
visual picture of any object diminishing, however, with
the increase in the distance to which it is removed, and the
amount of detail distinguishable in it following the same
proportion. Thus a man who looks across the street at a
placard posted on the opposite wall may very distinctly see
its general form and the arrangement of its heading, and may
be able to read what is set forth in its largest type, whilst
unable to separate the lines, stUl more to read the words,
of what is set forth below. But by crossing the street
so as to bring his eye nearer the picture he finds himself
able to read the smaller tyjje as easily as he before read
the larger, — the visual picture on his retina having been
magnified, say 10 times in linear dimension, by the
reduction of the distance of his eye from 40 feet to 4.
Similarly, if he holds a page of excessively minute type at
arm's length (<ay 40 inches) from his eye, he may be unable
to read it, not because his eye does not form a distinct
retinal picture of the page at that distance, but because
the details of that picture are too minute for him to
distinguish them. But if he brings the page from 40
inches to 10 inches distance, he may be able to read it
without difficulty,- — the retinal picture being enlarged four
times linear (or sixteen times superficial) by this approxi-
mation. Now the rays that enter the eye from each point
of a remote object diverge so little as to be virtually
parallel ; but the divergence increases with the approxima-
tion of the object to the eye, and at 10 inches the angle
of their divergence is as wide as permits the ordinary eye
to bring them to a focus on the retina. When the object
is approximated more closely, an automatic contraction of
the pupil takes place, so that the most diverging rays of
each pencil are cut off, and a distinct picture may be
formed (though not without a feeling of strain) when the
object is (say) from 5 to 8 inches distant, — giving still
greater minuteness of visual detail in conformity with the
increase of size. A further magnifj-ing power may be
obtained without the interposition of any lens, by looking
at an object, at 2 or 3 inches distance, through a pin-hole
in a card; for by thus cutting off the more divergent
rays of each pencil, so as to admit only those which can
be made to converge to a focus on the retina at that
distance, a distinct and detailed jncture may be obtained,
though at the expense of a great loss of light. Moreover,
MICROSCOPE
259
although an ordinary eye does not form a distinct picture
of an object at less than from 10 to 6 inches distance, a
" myopic " or " short-sighted " eye (whose greater refractive
power enables it to bring rays of wider divergence to a
focus on the retina) may form an equally distinct picture
of an object at from 5 to 3 inches distance ; and, as the
linear dimensions of that picture will be double that of the
preceding, the object will be " magnified " in that propor-
tion, and its details more clearly seen.
The effect of the interposition of a convex lens between
the eye and an object nearly approximated to it primarily
consists in its reduption in the divergence of the rays of
the pencils which issue from its several points, so that
they enter the eye at the moderate divgrgence which they
would have if the object were at the ordinary nearest limit
of distinct vision. And, since the shorter the focus of the
lens the more closely may the object be approximated to
the eye, the retinal picture is enlarged, causing the object
to appear maguitied in the same proportion. Not only,
however, are the component rays of each pencil brought
from divergence into convergence, but the course of the
pencils themselves is changed, so that they enter the eye
under an angle corresponding to that under which they
would have arrived from a larger object situated at a
greater distance ; and thus, as the picture formed upon the
retina by the small object ab, fig. 1, corresponds in all
Fio, 1. — Action of Simple Microscope.
respects with that which would have been made by the
same object AB of several times its linear dimension
viewed at the nearest ordinary limit of distinct vision, the
object is seen (by the formation of a " virtual image ") on
a magnified scale.
It is obvious that the " magnifying power " of any
convex lens so used is measured by the ratio between the
dimensions of the retinal picture formed with its assistance
and those of the picture formed by the unaided eye. Thus,
if by the use of a convex lens having 1 inch focal length
we can form a distinct retinal image of an object at only
an inch distance, this image will have ten times the
linear dimensions of that formed by the same object at a
distance of 10 inches, but will be only eight times as large
as the picture formed when the object can be seen by
ordinary vision at 8 inches distance, and only four times
as large as the picture of the same object formed by a
myojMc eye at a distance of 4 inches. It ig usual to
estimate the magnifying power of single lenses (or of com-
binations that are used as such) by the number of times that
their focal length is contained in 10 inches, — that of 1 inch
focus being thus taken as ten times, that of ^ inch as
one hundred times, and so on. But the rule is obviously
arbitrary, as the actual magnifying power varies in each
individual with the nearest limit of distinct vision. Thus
for the myopic who can see an object tlearly at 4 inches
distance, the magnifying powers of a 1 inch and ^ inch
lens will be only 4 and 40 respectively. The amplifying
power of every single convex lens, however, is impaired (1)
by that inability to bring to the same focus ihe rays which
fall upon the central and the'marginal parts of its surface
which is called "spherical aberration," and (2) by that
dispersion of the rays of different wave-lengths, in virtue
of their different refrangibihties, which produces coloured
fringes around the points and lines of the visual picturej
and is therefore caUed " chromatic aberration" (see Light).
These aberrations increase with the " angle of aperture ",
given to the lens, that is, with the proportion between the
diameter of its actual " opening " and the focal distance of
the object ; and thus, when a single lens of very short
focus is used in order to gain a high magnifying power,
such a reduction of its aperture by a perforated diaphragm
or "stop" becomes necessary (in order, by excluding
the peripheral rays, to obtain tolerable "definition"
^vith freedom from false colour) that the amount of
light admitted to the eye is so small as only to allow the
most transparent objects to be thus viewed, and these
only very imperfectly. In order to remedy this draw-
back, it was proposed by Sir D. Brewster to use instead
of glass, in the construction of simple microscopes, such
transparent minerals as have high refractive with low
dispersive power ; in which case the same optical effect
could be obtained with lenses of much lower curvature,
and the aperture might be proportionately enlarged. Thi«
combination of qualities is found in the diamond, whose
index of refraction bears such a proportion to that of glass
that a diamond lens having a radius of curvature of 8 would
give the same magnifying power as a glass lens whose radius
of ciTvature is 3, while the "longitudinal aberration"
(or distance between the foci of central and of marginal
rays) would be in a diamond lens only one-ninth of that
of a glass lens having the same power and aperture. Put-
ting aside, however, the costliness of the material and the
difficulty of working it, a source of imperfection arises from
a frequent want of homogeneousness in the diamond crystal,
which has proved sufficient to make a lens worked from it
give a double or even a triple image. Similar attempts
made by Mr Pritchard with sapphire proved more successful;
and, as a sapphire lens having a radius of curvature of 5
has the same focus and gives the same magnifying power
as a crown-glass lens having a radius of 3, it was found to
bear a much larger aperture without serious impairment
by either spherical or chromatic aberration. As the
sapphire, however, possesses the property of double refrac-
tion, the duplication of the markings of the object in their
retinal image constitutes a very serious drawback to the
utility of lenses constructed of this mineral; for, though
the double refraction may be reduced almost to nothing
by turning the convex side of the lens towards the object,
yet, as this is the worst position in regard to spherical
aberration, more is lost than is gained. Fortunately,
however, for biological investigators working with simple
microscopes, the introduction of the Wollaston doublet
superseded the necessity of any further attempts at turning
costly jewels to account as high-power magnifiers.
Wollaston Doublet. — This consists of a combination of
two plano-convex lenses, whose focal lengths (as directed by
Dr Wollaston) should be as 3 to 1, with their plane sides
turned towards the object, — the smaller lens being placed
lowest, and the upper lens at a distance of one and a half
times its focal length above it. This construction, how-
ever, has been subsequently improved — (1) by the introduc-
tion of a perforated diaphragm between the lenses ; (2) by
a more effective adjustment of the distance between the
two lenses, which seems to be most satisfactory when it
equals the difference of their respective focal lengths,
allowance being made for their thickness ; and (3) by the
division of the power of the lower lens (when a shorter
focus than .j^ inch is required) into two, so as to form
a "triplet." , AVhen combinations of this kind are well
260
MICROSCOPE
fjii^tnictecl, spherical aberration is almost wholly got rid
of, and chromatic dispersion is. so slight that the angle of
ai^rture may be considerably enlarged without much
sacrifice of distinctness. Such " doublets " and " triijlets,"
having been brought into use in England while the com-
pound microscope still retained its original imperfections,
proved very serviceable to such as were at that time
pjrosecuting min^ite biological investigations : for example,
the admirable researches of Dr Sharpey on ciliary action
in animals (1830-35) and Mr Henry Slack's beautifid
dissections of the elementary tissues of plants, as well as
his excellent observations on vegetable cyclosis (1831),
were made by their means. No one, however, would now
use Wollaston " doublets " or " triplets " of high power in
place of a compound achromatic microscope ; and for the
simple microscopes of low power that are usefid either for
dissecting or for picking out minute specimens (such as
diatoms) other constructions are preferable, as giving a
larger field and more light. As a hand-magnifier the
" Coddington " lens — which is a sphere of glass with a
deep groove ground out of its eciuatorial portion — has
many advantages.' By making this groove sufficiently
deep, both .spherical and chromatic aberrations can be
rendered almost insensible ; and, as the rays falling on any-
part of the spherical surface can only pass to the eye either
through or near the centre, the action of every part of that
surface is the same, so that the image of the object will be
equally distinct (when properly focussed) whether its parts
lie nearer to the axis of the sphere or more remote from it,
or the axis be itself turned to one side or the other. Again,
it was mathematically shown by Sir John Herschel in 1821
that by the combination of a meniscus with a double con-
vex lens — the four surfaces of these lenses having certain
proportionate curvatures — spherical aberration could be
entirely extinguished for rays ' parallel to the axis, the
combination being thus an "aplanatic" doublet, while
another combination, which he termed a " periscopic "
doublet, gives a remarkable range of oblique vision with
low powers, and almost entirely extinguishes chromatic
aberration, although at the expense of residual spherical
aberration. These combinations have been mounted both
as hand-magnifiers and as single microscojies, for both
which purposes they are much superior to single lenses of
the same magnifying power. But such combinations have
been greatly improved by the introduction of concaves of
flint glass, so as to render them achromatic as well as
aplanatic ; and nothing, according to the wTiter's experi-
ence, can now be used with greater advantage for all the
purposes answered either by the simple microscope or
the hand-magnifier than Browning's " platyscopic " lenses
or the "achromatic doublets" of Steinheil of ilunich.
Each of these combinations gives a large flat field, with
plenty of light, admirable definition, and freedom from
false colour.
At the perioa wncn " doublets" of very short focus were used in
order to obtain high maguifying jKiwer, it was requisite to mo\mt
these on such a stand as woulil enable the focal ailjustment to bo
made, and would admit the use of a special illuniinatiii'; apj^aratus
with great exactne-s-s. But now that comiiaiativcly low powers
©nly are employed tlie ordinary rack-aud-piiiiouniovemcnt is quite
Butficicnt for tlieir focal adjustnicut, and uotliing more is reciuired
* It is difficult to undcrstaud how the imuio of Coddington came to
be attached to the grooved sphere, seeing that he neither was nor
claimed to be the inventor of it. Dr Wollaston's first "doublet"
consisted of a pair of plano-convex lenses with their piano surfaces
opposed to each other, and a diaphragm with central aperture placed
between tliem. Sir D. Brewster showed that this construction is most
advantageous when the two lenses ni-e heniisi)lieres, and the central
aperture between their two plane surfaces is filled up by a transparent
cement having the same refractive index r.8 glass. And from this the
transition is obvious to the grooved sphere, which had been made for
Sir D. J^rewster long before the high commendation it received from
Mr Cuddingtou brought it into general repute. -
for the illumination of the object than a concave mirror beneith
the stage when it is transjiaicnt, and a condensing lens above when
it is oitaque. The vaiious patterns of simple microscope now mado
by ditlerent makers vary in their construction, chiefly in regard to
portability, the size of their stages, aud tlie mode in which " re»ta"
or supports to the hands are provided. Tliese, in Continental in-
struments, arc very comuiouly attached to the stage ; but, unless
the stage itself and t!ie pillar to whicli it is fixed are extremely
massive, the resting of the hands ou the supports i$ apt to depress
tht stage in a degree that aflccts the local adjustment ; and where
portability is not an object it seems better that the hand-supports
sliould be independent of the stage. For a laboratory microscoi>e,
the pattern represented iu fig. 2 has been found very convcniont, —
the framework beioz of mahogany or other hard wood, the stage
^i^
Fig. 2,
being large enough to admit a dissection or carry a water-trough
of considerable size, aud the bent aiTO that can'ics the "powers"
being made capable of revereion, so as to permit the use of lenses
of very long as well as of very short focus. As it is desirable that
the stage should not be acted on chemically by sea-water, acids, or
other reagents, it may be made either of a square of plate-glass or o(
a plate of ebonite with an apertui-e in the middle ; and cither of
these may be made to slide iu grooves in the side supports, so that
one may be substituted for the other. The ami may be easily
made (if desired) to carry the body of a compound microscope, so
as to apply it to the examination of objects dissected or othcrwiso
prepared under the simple microscope, without transferring them
to another instrument. A portable form of simidc microscope is
shown in fig. 30.
Compound iticroicope. — The placing of two convex lenses
in such relative positions that one should magnify an
enlarged image of a small near object formed by the other
naturally soon followed the invention of the telescope, and
seems to have first occurred to Hans Zansz or his son
Zacharias Zansz, spectacle-makers at Mi.ldelburg in Hol-
land, about l.'iOO. One of their compound microscope.',
which they presented to Prince Maurice, was in the year
1G17 in the possession of Cornelius Drebell of Alkmaar,
who then resided in London as mathematician to king
James I. In order to make clear the successive stages by
which the rude and imperfect microscope of that period
has, after remaining for two centuries unimproved in any
essential particular, been developed within the last half-
century into one of the most important instruments of
scientific research that the combination of theoretical
acumen and manipulative skill has ever produced, it i^«
necessary to explain the principle of its construction, and
to show wherein lay the imperfection of its earlier form.
In its simplest con.struction, as already stated, tho
comix)und microscope consists of only two lenses, — tho
"object-glass" CD, fig. 3, which receives the light-rays direct
from the object AB placed near it, and forms an enlarged
but reversed image A'B' at a greater distance on the other
side, and tlie "eye-glass" LM, which receives the rays that
diverge from the several points of this image as if they,
proceeded from the iioints of an actual object occupying
the position and enlarged to the dimensions A'B', and
.brings these to the eye at E, so altering their course as to
MICROSCOPE
261
«ct as & simple microtcope in magnifying that image to the
observer. It was early found useful, however, to interpose
another lens FF, fig. 4 (the " field-glass "), between the
object-glass and the image formed by it, for the purpose
of giving such a slight convergence to the pencil of rays as
shall reduce the dimensions of the image, and thus allow
a larger part of it to come within the range of the eye-
flG. 3.— Di;igram of Siiinilest
FoiT) of Cooipou&d Micro-
— Diagrnui of Complete
Compound Microscope.
glass, so that more of the object can be seen at once.
And it was soon perceived that the eye-glass and the
field-glass might be advantageously combined into an
"eye-piece," in which a perforated diaphragm might be
inserted at the focal plane of the image (i.e., in the focus of
the eye-glass), so as, by cutting ofi the peripheral portion
of the field of view, to limit it to what can be seen with
tolerable distinctness.
It is obvious that the magnifying power of such an
instrument would depend (I) on the proportion between
the size of the image formed at BB and that of the
actual object, and (2) upon the magnifj-ing power of the
eye-glass. And further the proportion which the size of
the image bears to that of the object depends upon two
factors, — (1) the focal length of the object-glass, and
(2) the distance between the object-glass and the plane
BB occupied by the image it forms. If we diminish
the focal length of the object-glass, the object must be
brought nearer to it, so that, while the distance of the
image on the other side remains unchanged, that distance
comes to bear a larger proportion to the distance of the
otject, and the sizo of the image is augmented in a cor-
responding ratio. On the other hand, the object-glass
remaining unchanged, the distance at which it forms the
image of the object can be increased by a lengthening of the
tube of the microscope ; and, as this involves a shortening
of tho distance between the object-glass and the object, the
proportion which the former bears to the latter is augmented,
and the image is correspondingly enlarged. Thus an
increase in the magnifying power of the compound micro-,
scope may be gained in three modes, which may be used
either separately or in double or triple combination, — viz.,
(1) shortening the focus of the object-glass, (2) lengthening
the tube of the microscope, and (3) increasing the magnify-
ing power of the eye-glass by shortening its focus. This,
it may be remarked, also lengthens the distance of the
image from the object-glass, by bringing the focal plane
BB nearer the eye-glass. The second of these methods
was not unfrequently used in the older microscopes, which
were sometimes made to draw out like telescopes, so as to
increase the amplifying power of their object-glasses. But,
whilst very inconvenient to the observer, such a lengthen-
ing of the one distance involved such a shortening of the
other as greatly impaired the distinctness of the image by
increasing the aberrations of the object-glass, so that this
method came to be generally abandoned for one of the other
two.
When lenses of from 1 to 4 inches focus were used as
object-glasses, and their apertures were restricted by a stop
to the central part of each, tolerably distinct images were
given of the larger structural arrangements of such objects as
s.ections of wood or the more transparent wings of insects, —
which images would beer a further moderate gnlargement
by the eye-glass without any serious deterioration either by
want of definition or the introduction of colour-fringes.
But when lenses of less than 1 inch focus were employed
in order to obtain a higher magnifying power, the greater
obliquity of the rays so greatly increased their aberrations
that defective definition and the introduction of false
colours went far to nullify any advantage obtainable from
the higher amplification ; while the limitation of the
aperture required to keep these aberrations within even
moderate limits occasioned such a loss of light as most
seriously to detract from the value of the picture. On the
other hand, the use of deeper eye-pieces to enlarge the
images formed by the object-glasses not only brought out
more strongly all the defects of those images, but introduced
a new set of errors of their own, so that very little was
gained by that mode of amplification. Hence many of the
best of the older microscopists (notably Leettwenhoek,
q.v.) made some of their most valuable discoveries by the
use of the simple microscope; and the amount of excellent
work thus done surprises every' one who studies the history^
of microscopic inquiry. This was still more the case, as
already stated, when the use of single lenses of very short
focus was superseded by the introduction of the Wollaston
doublet. And the substitution of these doublets for the
single lenses of object-glasses, while the single lens of the
eye-glass was replaced by a Herschel's aplanatic doublet,
and the field-glass was a convex lens whose two curves had
the proportion of 1 : 6 (the form of least spherical aberra-
tion), constituted the greatest improvement of which, the
instrument seemed capable in pre-achromatic times. i(
It has been only within the last sixty years (1820-30)
that the microscope has undergone the important improve-
ment which had been worked out by Dollond in the
refracting telescope more than sixty years previously, — •
namely, the correction of the chromatic aberration of its
objectives by the combination of concave lenses of flinfri
* This combination was made in the first microscope of which th*
writer became possessed, about the year 1830 ; and he well recollect?
the great superiority to any compound microscope of the old coustrac^
tion which was proved by its power of separating the lines oa the
Menelaus scale, and of bringing into view the details of the structure of
animalcules, with a clearness that only an achromatized obj«ct-glbS4
could surpass.
202
MICROSCOPE
glass with convex lenses of crown, wluie their spherical
aberration is corrected by the combination (as in Herschel's
aplanatic doublet) of convex and concave surfaces o;
different curvatures. The minute size and high curvature
of the lenses required as microscopic objectives were long
considered as altogether precluding the possibility of success
in the production of such' combinations, more especially
as the conditions they would have to meet differ altogether
from those under which telescopic object-glasses are
employed. For the rays from distant objects fall upon the
latter with virtual parallelism ; and the higher the power
required the longer is the focus given to them, and the
smaller is the deflexion of the rays. In the microscope, on
the other hand, the object is so closely approximated to the
objective that the rays which proceed to it from the latter
have always a very considerable divergence ; and the
deflexion to which they are subjected increases with that
reduction of the focal length of the objective which is
the necessary condition of the increase of its magnifying
power. And thus, although the telescopic "triplet"
worked out by DoUond (consisting of a double-concave of
flint glass, interposed between two double-convex lenses of
crown) can be so constructed as to be not only completely
aplanatic (or free from spherical aberration) but almost
completely achromatic (or free from chromatic aberration),
this construction is only suitable for microscopic objectives
of long focus and small angular aperture, the rays falling
on which have but a very moderate divergence. And
though, as will presently appear, some of the early attempts
at the achromatization of the microscope were made in
this direction, it was soon abandoned for other plans of
construction, which were found to be alike theoretically
and practically superior.
It seems to have been by Professor Amici, then of
Modena, about 1812, that the first attempts were made at
the achromatization of microscopic objectives ; but, these
attempts not proving successful, he turned his attention to
the production of a reflecting microscope, which was a
decided improvement upon the non-achromatized compound
microscopes then in use. In the year 1820, however, the
subject was taken up by Selligues and Chevalier of Paris,
who adopted the plan of superposing three or four com-
binations, each consisting of a double-convex of crown
cemented to a plano-concave of flint, The back combina-
tion (that nearest to the eye) was of somewhat lower power
than those placed in front of it, but these last were all of
the same focus, and no attempt was made by these opticians
to vary the construction of the several pairs thus united,
80 as to make them correct each others' aberrations.
Hence, although a considerable magnifying power could
be thus obtained, with an almost complete extinction of
chromatic aberration, the aperture of these objectives
could not be greatly widened without the impairment of
the distinctness of the image by a "coma" proceeding
from uncorrected spherical aberration.
In ignorance, it would appear, of what was being done
by the Paris opticians, and at the instigation of Dr Goring
(a scientific amateur), Mr TuUey — well known in London
as an able constructor of telescopic objectives — began,
about the year 1824, to work object-glasses for the micro-
scoiie on the telescopic plan. After many trials ' he
succeeded, in 182.'), in producing a triplet of .j?^ inch focus,
admitting a pencil of 18°, which was so well corrected as
to perform very satisfactorily with an eye-piece giving a
magnifying power of 120 diameters. He afterwards made
a similar triplet of shorter focus, which, when placed in
* It ia due to Mr Joseph J. Lister to mention that Tullcy's final
success with this low power seems to have been attained by working
on a suggestion given him by that genl\eman. See Mmtliti/ Micro-
teopical Journal, vol. iii. (1870), p. Mi.
front of tne previous one, increased the angle- !)f the -trans-
mitted pencil to 38°, and !>"■■« an eye-piece giving 'a
magnifying power of 300 diaiieter.s. These triplets are
said by Mr Ross to have never been excAded by any similar
combinations for accurate correction throughout the field. '
Having come into possessionj at the end of 1826, of
an objective of Chevalier's construction, Mr J. J. Lister
carefully examined its 'properties, and compared them with
those of TuUey's triplets ; and this comparison having led
him to institute further experiments he obtained results
which were at first so conflicting that they must have
proved utterly bewildering to a less acute mind,^ but ■^hich
finally led him to the enunciation of the principle on which
all the best microscopic objectives are now constructed.
For he discovered that the performance of such com-
posite objectives greatly depends upon the relative position
of their component combinations, — the effect of the flint
plano-concave upon the spherical aberration produced by
the double-convex of crown varying remarkably according
to the distance of the luminous point from the front of the
objective.. If the radiant is at a considerable distance, tlTe
vays proceeding from it have their spherical error under-
corrected ; but, as the source of light is brought nearer to
the glass, the flint lens produces greater proportionate
effect, and the under-correction diminishes, until at length
a point is reached where it disappears entirely, the rays
being all brought to one point at the conjugate focus of
the lens. This, then, is one aplanatic focus. If, however,
the luminous point is brought still nearer to the glass, the
influence of the flint continues for a time to increase, and
the opposite condition of over-correction shows itself. , But,'
on still further approximation of the radiant, the, flint
comes to operate with less effect, the excess of correction
diminishes and at a point still nearer to the glass vanishes,*
and a second aplanatic focus, appears. ^From this point
onwards under-correction takes the place of over-correction,^
and increases till the object touches the surf ace . of , the-
glass. As every such doublet, therefore, has two aplanatic
foci for all points between which it is over-corrected, while
for all points beyond it is under-corrected, the optician is
enabled to combine two or more doublets with f perfect
security against spherical error. This will beientirely
avoided if the rays be received by the front glass from its
shorter aplanatic focus, and transmitted through the back
glass in the direction of its longer aplanatic pencil.WBy
the approximation of the two doublets over-correction will
be reduced, while their separation will produce under-cor-
rection ; and thus, by merely varying the distance between
two such combinations, the correction of . the spherical
error may be either increased or diminished according to a
definite rule. Slight defects in one glass may thus be
remedied by simply altering its position in relation to the
other, — an alteration which may be made with very little
disturbance of the colour-correction. ■ This important
principle was developed and illustrated by Mr Lister in a
memoir read to the Royal Society on January 2J, 1830,
On some Properties in Achromatic Object-glasses, applicable
to the Improvement of the Microscope ; and it was by work-
ing on the lines there laid down that the three London
opticians Ross,' Powell, and James Smith soon pro-
' Thus he found that, while each of Chevalier's doublet combina-
tions, when used siugly, presented a "bur" or "coma" outwards,
this coma, instead of being exaggerated by the combination of two of
these doublets, was much diminished. Or the other hand, while
two of Tulley's triplets, each of which performed admirably by
itself, were used together, the images of all objects not in the centre
presented a strong bur inwards with an under-correction of colour^ i§M
3 In 1837 Mr Lister gave Mr Ross a projection for an objective of
\ inch focus, in which a triple front was combined with two doublets.
The great superiority of this lens, admirably executed by Mr Ross, caused*
him to adopt its plan as the standard one for high powers; and it is still
in general use, — the back leus aUo being sometimes made as a tripleL
MICROSCOPE
263
laced microscopic objectives that surpassed any then con-
itruct^ on the Continent, while the subsequent adoption
of the same principles by French and German opticians,
as also by Professor Amici x)f Florence, soon raised their
objectives to a corresponding level.
It has proved more advantageous in practice to
make the several components of an achromatic objective
correct each others' aberrations than to attempt to render
each perfect in itself; and the mode in which this is
accomplished will vary with the focus and angiilar aperture
given to each combination. Thus, whOe a single " telescopic
triplet " answers very well for the lowest power usually
made (4 inches focus), and the same plan may be used —
though at the sacrifice of angular aperture — for objectives
of 3 inches, 2 inches, and even 1 inch focus, the best per-
formance of these powers requires the combination of two
doublets. And, while this last system also serves for
objectives of f inch and J inch of low angle, a third com-
ponent is required for giving to these objectives the
aperture that renders them most serviceable, as well as for
all higher powers. Instead of combining three achromatic
doublets, however, many makers prefer placing in front a
plano<onvex of crOFn, and adding a third lens of crown to
the doublet at the back, still using a doublet in the middle, —
the whole combination thus consisting of six lenses, four
of crown and two of flint. Further, Mr Wenham has
shown that the whole colour-correction may be effected in
the middle by interposing a double concave of dense flint
between two double-convex lenses of crown, — the back lens,
as well as the front, being then a plano-convex of crown,
making five lenses in all. This plan of construction, though
suitable to objectives of moderate angular aperture, and
advantageous in regard to comparative simplicity and
economy of construction, does not seem so well adapted for
objectives to which the largest attainable aperture is to be
given, — these being usually constructed with a triplet in
front, a doublet in the middle, and a triplet at the back, so
as to consist of eight separate lenses. And the first-class
constructors of achromatic objectives in the United States
usually place in front of these, in their highest powers, a
single plano-convex of crown, by the addition of which a
greater working distance can be obtained. But, as every
such addition increases the liability to error from imper-
fections in the centring and grinding of the lenses (as
well as loss of light by the partial reflexion of oblique
rays from their surfaces), it is obvious that the most exact
workmanship, involving a proportionate costliness, is
required to bring out the full effect of such complex con-
struction. And where angular aperture is regarded as the
quality of primary importance it will be usually found
preferable to have recourse to objectives constructed on
either the " water " or the " oil " immersion system, to be
presently described.
The great increase thus attained in the perfection
of the corrections of microscopic objectives for both
spherical and chromatic aberration of course rendered
it possible to make a corresponding increase in their
angular aperture. The minute scales of the wings of
butterflies and other insects were naturally among the
objects much examined ; and it was soon perceived that
certain lines and other markings became clearly discernible
on these scales with objectives of what was then considered
large angle which were utterly undistinguishable with
non-achromatized microscopes (however high their magnify-
ing power), and very imperfectly shown under achromatic
objectives of small angle. Hence these scales came to be
used as " tesfcobjects," for judging of the " definition " and
" resolving power " of microscopic objectives, — the former J
property consisting in the clearness, sharpness, and freedom
from false colour of the microscopic images of boundary I
lines, ana depending on the accuracy with which the aber-
rations are corrected, while the latter term designates that
power of separating very closely approximated markings
which is now known to be a
"function" of aperture. The
insect-scales formerly most valued
for these purposes were those of
the Morpko menelaus (fig. 5) and
the similarly lined scales of the
Polyommatus argus (a2ure-blue),
the "battledoor" scales of the
same butterfly (fig. 6), the ribbed
scales of the Lepisma sacckarina
(sugar-louse), and the minute and
jjeculiarly marked scales of the
Zepidocyrtus curvicollis (fig. 7),
commonly known as the Podura.
The writer recollects the time
when the satisfactory "resolu-
tion " of the first, three of these
tests w^as considered a suflScient
proof of the goodness of even
high-power objectives, and when
the Porfura-markings, if visible at all, could only be dia-,
tinguished as striae. The further opening-out of the
aperture, however, enabled these strias
to be resolved into rows of " exclama-
tion marks " ; and, while there is still
some uncertainty as to the precise If
structure of which these markings are j
the optical expression, practical op-
ticians are generally agreed that the
/"orfwra-scale is very useful as a test
for definition, with even the highest
objectives, though it only serves as a
test for a very moderate degree of re-
solving power. For the latter purpose
it has been completely superseded by
the closely approximated markings of
the siUcified envelopes of certain p,g g _ Battledoor
diatoms (which, however, show them Scale of Polyomma-
selves in very different aspects accord '"" argus.
ing to the conditions under which they are viewea, figs.
8-11), and also by lines artificially ruled on glass, as ia
Nobert's "test-plate," the number *
of lines in the nineteen bands of
which is stated by M. Nobert
to range from 1000 to 10,000
to a Paris line, while Dr Royston
Pigott gives the numbers in an
English inch as 11,529 to the inch
in the first band, and 112,595
in the nineteenth. This last
dimension (as will afterwards
appear} approaches the minimum
distance at which such markings
are theoretically separable by any
magnifying power of the micro-
scope.
The enlargement of the angle
of aperture of microscopic ob-
jectives and the greater complete-
ness of their corrections, which
were obtained in the first in- Fio. 7.— Test-Scales of Podur»
stance by the adoption of Mr ^J::^i^^tZ>47'^i^
Lister s principles, and were de- scale ; B, email scale mor»
monstrated by the resolution of ftiotly marked,
the test-objects then in use, soon rendered sensible fta
imperfection in their performance under certain circum-
stances, which had previously passed unnoticed; and th^
264
MICROSCOPE
important discovery was made by Mr Andrew Ross that
a very decided difference exists in the precision of the
image according as the object is viewed with or mthout
a covering of thin glass, as also according as this cover is
thin or thick. ^ As this difference increases in proportion
to the widening of the aperture, it would obviously be a
TfUff Tf
; :E 5
. - -s -
i±i
:: =
zl'il't
=1
: : 5
! ; s
I', s
= : : : ® ^gp
iig. 10. Fig. n.
Portions of Siliceous Valve of Pleurosi^p^ia angnlatum, from a Photo-
graph taken by Central Illumination. Magnified 2000 diametei-s.
source of great error and embarrassment if a means could
not be found for its rectification. Its optical source, how-
ever, having been found by Mr Ross to lie in the
."negative aberration" which is produced in the rays
proceeding from the object to the front glass of the objec-
tive by the interposition of the plane-glass cover, and
which increases with its thickness, his practical ability
enabled him at the same tinte to indicate the remedy,
which consists in under-correcting the front lens and over-
correcting the two pos-
terior combinations, and
in making the distance
between the former and
the latter capable of
adjustment by means of
a screw-collar, as sho\ra
in fig. 12. For when^
the front pair is approxi- g
mated most nearly to the
next, and its distance
from the object is in-
creased, its excess of
positive aberration is
more strongly exerted
upon the other two pairs
than it is in the con-Fio. 12.— Section of Ailjusting Achromatic
trary conditions, and 0'^J''"='-G'''»»- A, uncovered ; B, covcr«L
thus neutralizes the negative aberration produced by the
interposition of the covering-glass. This correction is not
needed for objectives of .low or medium jiower and small
angle of aperture ; but it should always bo provided when
the angle exceeds 50°, — unless (as is now generally done
' Trans. Soc. of Arts, vol. li
in the case of objectives constnicted . for students' use)
the maker adjusts them originally, not for uncovered
objects, but for objects covered with glass of a standard
thickness, say 000.5 or 0-004 inch. A departure from
that standard to the extent of one or two thousandths of
an inch in either direction, though extremely injurious
to the performance of objectives whoso aperture is 125° or
more, scarcely makes itself perceptible in those of 90° or
100°. And the .same may be said in regard to the
immersion-objectives next to be described, which are
peculiarly suitable to the purposes of minute histological
research.
Immersion System. — It was long since pomted out by
Professor Amici that the introduction of a drop of water
between the front surface of the objective and either the
object itself or its covering-glass would diminish the loss
of light resulting from the pas.sage of the rays from the
object or its covering-glass into air, and from air into the
front glass of the objective. It was obvious to him, more-
over, that when the rays enter the object-glass from water,
instead of from air, both its refractive and its dispersive
action will be so gi-catly changed as to need an important
constructive modification to meet the new condition. This
modification seems never to have been successfully effected
by Amici himself ; but his idea was taken up by the two
eminent Paris opticians, JlJf. Hartnack and Nachet, who
showed that the application of what is now known as the
" immersion system " to objectives of short focus and large
angular aperture is attended, not merely with the advan-
tages expected by Professor Amici, but with others on which
he did not reckon. As the loss of light by the reflexion of
a portion of the incident rays increases with the obliquity
of their incidence, and as the proportional loss is far smaller
when the oblique rays pass into glass from water than
when they enter it from air, the advantage of increas-
ing the angular aperture is more fully experienced
with "immersion" than with "dry" objectives, — just as
Professor Amici anticipated. But, further, the immer-
sion system allows of a greater working distance between
the objective and the object than can bo attained ■with a
dry or air objective having the same angular aperture ;
and this increase affords not only a greater freedom of
manipulation, but also a greater range of " penetration "
or " focal dejjth." Purther, the observer is rendered so
much less dependent upon the exactness of his cover-
correction that it is found that water-immersion objectives
of high power and considerable angular aperture, extremely
well adapted for the ordinary purposes of scientific inves-
tigation, can -be constructed without it, — a small departure
from the standard thickness of covering-glass to which such
olijectives are adjusted by the maker having scarcely any
effect u[)on the distinctness of the image. It is now the
practice of several makers to supjily two fronts to objectives
of Yjs °'' tV '""^^ focus, one of them fitting the objective for
use "dry" (that is, in air), whilst the substitution of the
other converts it into a water-immersion objective. And
in the Objectives constructed on Mr Wenham's system no
change in the front glass is needed, all that is necessary for
nmking them work a>i immersion-lenses being a yet closer
aijjiroximation of th front lens to the second combination,
which can be made by the screw-collar.
Within the last few years, however, tne immersion
system has undergone a still further and most important
development, by the adoption of a method originally
suggested by Mr W^nham (though never carried out by
him), and independently suggested by Mr Stephenson to
Professor Abbe of Jena, under whose direction it w^as first
worked out by Zeiss (the very able optician of Jena), who
has been followed by Powell and Lcaland of London, as
well as by several other constructors of achromatic objec-
MICROSCOPE
265
tives both in England and " elsewhere, with complete
success. This metiod cousiste in the replacement of the
water previously interposed between the covering-glass and
the front glass of the objective by a liquid having the same
refractive and dispersive powers as crown-glass, so that the
rays issuing at any angle from the upper plane surface of
the covering-glass shall enter the plane front of the objec-
tive, without any deflexion from their straight course, and
without any sensible loss by reflexion, — even the most
oblique rays that proceed from the object keeping ■ their
direction unchanged until they meet the back or convex
surface of the front lens of the objective. It is obvious
that all the advantages derivable from the system of water-
imhiersiou will be still more thoroughly attained by this
system of " homogeneous " immersion, provided that a fluid
can be obtained which meets its requirements. After a
long course of experiments. Professor Abbe found that oil
of cedar wood so nearly corresponds with cro\vn-glass, alike
in refractive and in dispersive power, as to serve the
Itarixjse extremely well, except when it is desired to take
si>ecial advantage of the most divergent or marginal rays,
oil of fennel being then preferable. There are, however,
strong objections to the use of these essential oils in the
ordinary work of research ; and it seems not unlikely that
a solution of some one or more saline substances will be
found more suitable. -■ In addition to the benefit conferred
by the water-immersion system, ' and more completely
attained with the homogeneous, it may be specially pointed
out that, as no correction for the thickness of the covering-
glass is here required, the microsoopist can feel assured
that he has such a view of his object as only the most per-
fect correction of an air-objective can afford. This is a
matter of no small importance, for while, in looking at a
known object, the practised microscopist can so adjust his
air-objective to the thickness "o/ .its covering-glass as to
bring out its best performance, he cannot be sure, iu regard
to an unknown object, what appearances it ought to pre-
sent, and may be led by imperfect cover-correction to au
erroueous conception of its structure.
It has been recently argiieJ that, as tlio slightest variation in the
rcfi-activc inJex of either the immersion fluid or tlie covering-glass,
a change of eye-i>icces, or the least alteration in tlie length of the
hoily — in a woi-.l, any circumstances ditrciing in the slightest degiee
ftom tliosc under whicli tiie objective was corrected — must atiect
the [wrformanL-e of Itoniogencous-immcrsion objectives of the highest
class, Oioy sl-.ould still Lc made adjustable. The truth of this
contention can, no doubt, be proved, not only theoretically, but
liractically, — the introduction of the adjustment enabling an experi-
enced manipulator to attain the highest degree of perfection in the
exhibition of many mounted objects, which cannot be so well sliown
with objectives in fixed settings. But it may well be questioned
.whether it is likely to do the same service in the hands of an ordi-
nary working liistologist, and whether the scientific investigator will
not linil it preferable, w-hcn using these objectives, to acceptwhat their
maker lias li.xcd as their ]ioint of best pciformancc. The princijial
source of error in his employment of them lies in the thickness of tlio
optical section of the object; for the rays proceeding fron» its deeper
plane, having to pass through a< ineiliuni intervening between that
I'lane and the cover-glass, whoso refinctive and dis]><;i-sivc indices
dillVr from those of the glass and inimcniion -fluid, cannot be
bi-ought to so aecumte a focus as tliosc proceeding from the plane
inmiediatcly beneath the cover-glass. The remedy for this, how-
ever, seems to lie rather in making tlic preparation as tliin as
possible than in the introduction of what is likely, in any but the
most skilful and e.xiierienoed Iian.Is, to prove a new source of error.
Every one who has examined muscular fibre, for example, under a
dry obji'ctivc of very high power ajul largo aperture, well knows
that so gri-atan alteration i«]>roduced in its aspect by the sliglitest
changf in either the focal adjustment or tlie cover-conection
that it is im|iossibIc to say witli certainty what arc the apjiear-
Mices whii h give the most correct optical expression of its structure.
I'hU being a matter of judgment on the part of each observ.r, it
M#lns obvious that the nearest approach to a correct view will be
pi^lnbly given by the focal adjiutment of the best homogeneous
iinnicrsion-objectivcs, in fixed settings, to tlic plane of the prepara-'
lion immediately beneath tho cover-glass (see Jour. Koy. Micros.
Pot ,.1882, pp. 407, 854, SC)
In every particular in which the ■water-immersion
system is superior to the dry, • it is itself surpassed by
the oil or other homogeneous system, the anticipa-
tions of those by whom it was suggested being thus fully
realized. -But the advantages already spoken of as deriv-
able from the use of the " immersion system " are altogether
surpassed by that which the theoretical studies of Professor
Abbe have led him to assign to it, and of which he has
practically demonstrated its possession. For he has shown
(as will be explained below) that the interposition of either
water or oil so greatly increases the real " aperture " of
the objective that immersion-objectives may be constructed
having a far greater virtual aperture than even the theo-
retical maximum (180°) of the angulai aperture of an
air-objective.
The same eminent physicist, working on the basis
supplied by the mathematical investigations of Professor
Helmholtz and himself on the undulatory theory of light,'
has further established an entirely new doctrine in regard
to the production of highly magnified representations of
closely approximated markings. -All that has hitherto
been said of the formation of images by the compound
microscope relates to such as are produced, in accordance
with the laws of refraction, by the alteration in direction
which the light-rays undergo in. their passage through the
lenses interposed between the object and the eye. These
dioptric images, when formed by lenses free from spherical
and chromatic aberration,.are geometrically correct pictures,'
truly representing the appearances which the objects them-
selves would present were they enlarged to the same scale
and viewed under similar illumination.- And we seein
justified, therefore, in drawing from such microscopic
images the same conclusions in regard to the objects they
picture as we should draw from the direct vision of acfcual
objects having the same dimensions. The principal source of
error in such interpretations arises out of the "interference "
to which the rays of light are subjected along the edges of
the minute objects through which they pass, or along any
such lines or margins in their inner part as are sufficiently
opaque to throw a definite shadow. For every such
shadow must be bordered, more or less obviously, by inter-
ference- or diffraction-spectra; and thus the images of
strongly-lined objects with very transparent intermediate
spaces may be so troubled or confused by these " diffraction-
spectra " as to Vender it very doubtful what interpretatitn
is to be put upon their appearances.
A good example of this kind is aflbrdcd by tho scaie3''of the
gnat or mosquito, which are composed of a vei-y delicate double
membrane, strengthened by longitudinal ribs on both sides, those
of tho opposite sides uniting at tlie broad end of the scale, wlijre
they generally terminate as bustle-shaped appendages beyond the
intermediate membrane. These are crossed by fine markings, which
are probably ridge-like cornigations of the membrane, common to
both sides of the scale. Between each pair of longitudinal ridges
there niay be seen, under certain adjustments of focus and illumi-
nation, three unifoi-nv pai-allel rows of beads, whidt have been
supi'oscd to represent a true structure iu the membrane. By Dr,
AVoodward (colonel in the United States aimy), however, it has been'
sliown tliat this beaded appearance is merely the i-esult of the "inter-
ferences " produced by the longitudinal and trai»vcrse lines of the
scale. For the longitmlinal dilfractionlines are clearly seen, alike
in the mioroscoiiic image and in photographs (fig. 13), to extend into
emi>ty space l>eyond the contour of the scales, almost as far as, the
ends of the biistles iu whidi the parallel ribs terminate;-. and
tliey vary in number with tho varying obliquity of illumination, so
that in tlie same stale two, three, four, or even five rows of beads
can be seen, and iihotographcdiSt pleasura. infvtry intercostal
si>acc. *
Every microscopist jwho' Has. worKed mucn witli' high
Ijowcrs is Well aware of the difficulty of distingufshirig
between real and spectral markings, — a difficulty which can
only be overcome by training and exjierience. *, It seems.
> Mo.dMj ilii
(1876), p. 263
XVI. — -u
260
MICROSCOPE
however, to have been now fully ascertained by Pro-
fessor Abbe that it is only through such diffraction-spectra
that the microscope can make us acquainted with the
minutest structural features of objects, since, according
to the calculations of Professor Helmholtz and himself
(based on the constants of the undulatory theory), no
amount of magnifying power can separate dioptrically two
lines, apertures, or markings of any kind, not more than
:; s'o 0 "' ^° i"ch apart. The visual differentiation or
" resolutipn " of lines or other markings whose distance lies
their dillraction-spectra,' and that the confidence to b«
placed in the latter class of representations will be greatei
in proportion to the completeness of the recombination of
the separated interference-spectra, which, again, will be
proportional (accurate correction of the aberrations being
assumed) to the aperture of the objectivc.-
The combined advance of scientific theory and of
practical skill in the application of it have now brought
up the compound achromatic microscoiie to an oi>tical per-
fection that renders it capable of actually doing almost
everything of which, in the present state of optical
theory, it can be regarded as capable. The resolution
of Nobert's nineteenth band, having 112,595 lines
to an inch, which was long regarded as the crux of
microscopists, is now found so ea.sy as to leave little
room for doubt that, if a new, test were obtainable
having the minimum vlsihile. of 118,000 lines to the
inch, an oil-immersion objective would be found to
resolve it. But the experience of the past makes it
evident that, as no limit can be set to the advance
of optical theory, results yet more remarkable may be
still exi)ected to arise, every such advance beiiig turned
Ehowing Beailcd Markings rroduced by Diffraot:on; to account by the practical skill which exjierience has
7. -J J ^^^ enabled the best constructors of achromatic ob-
FlO. 13.— Scale (
Irom a rhotograjjh by Colonel Dr"Woodward.
within that limit is entirely the result of " interference," —
the objective receiving and transmitting, not only dioptric
rays, but the inflected rays whose course has been altered
in their passage through the object by the peculiar disposi-
tion of its particles, and combining these rays into a series
of diffraction-spectra, the number and relative position of
which bear a relation to the structural arrangement on
which their production depends. If the objective be per-
fectly corrected, and all the diffraction-spectra lie within
its field, these will be recombined by the eye-piece so as to
form a secondary or " diffraction " image, lying in the same
plane with the dioptric image, and coinciding with it, while
filling up its outlines by supplying intermediate details.
But where the markings (of whatever nature) are so closely
approximated as to produce a wide dispersion of the inter-
ference-spectra, only a part of them may fall within the
range of the objective ; and the recombination of these by
the eye-piece may produce a diffraction-image differing
more or less completely (perhaps e\en totally) from the
real structure; while, if they should lie entirely outside
the field of the objective, no secondary or diffraction image
will be produced. And thus, while the general form of
such an object as a diatom-valve may be correctly given in
a dioptric image, its surface may ajipear quite unmarked
under an objective of small aperture, however great its
magnifying power, though covered with regulaily disposed
markings when seen through an objective of wider aperture i ''■*' nearly all er
with perhaps only half the magnifying power. "'""■ *" "'"' *''" '''""
It is obvious, however, that, while the dioptric image
represents the actual object, the diffraction-image thus
formed by the reunion of a portion of the interference
pencils is only an optical expression of the result of thair
partial recombination, which may represent something
«nurely different from the real structure. For it has been
proved experimentally, by placing finely-ruled gratings in
the position of object-s, and by limiting the apertures of
objectives by diaphragms with variously disposed perfora-
tions, that the same arrangement of lines shall bti presented
to the eye by differently lined surfaces, and different
arrangements by similarly lined surfarc.-i, according to the
numbers and relative positions of the reunited spectra.
Hence it is clear that there must bo an essential difference
in character and trustworthiness between the images
dioptrically formed of the general outlines and larger
iletails of inicroscoijic objects and those representations, of
their finer details which are given by the recombination of
jectives to attain. ^
Tlie progressive iinprovemeaits thus effcotoJ in the construction
of uiicrosropic objectives have bccu accompanied by other iuiprovo-
ments, alike in tlio optical and in tlio mechanical anangements by
which tlie best peifoiuiance of these objectives can bo secured; and
it will be desiiable now to describe in succesbion tlio most apjiroved
forms of the eyo-picco, tlio objective, and tlie illuminating apparatus
respectively, and then those of the iiistiument as a whole, point-
ing out tlio special adaptiveiioss of each to the requiremciits of
ditli^eut classes of scientiiic investigators.
Ete-Pieces.
It very early became obvious to thosw who were engaged ia
tli« achromatization of microscopic objectives that their best
porfoi-manco was obt.aincd wlien the image given by them was
further enlarged by the eye-piece known as tlio Huygcnian, as
having been devised by Huygens for his telescopes. It cojiaists
of hvo planoconvex lenses (EE and FF, fig. 4), with tlieir plane
sides towards the eye ; these are placed at a distance c/jual to hall
the sum of dieir local lengths, — or, to speak with more jireoision,
at half the sum of the focal length of the eye-glass, and of tho dis
tinco from tho field-glass at which an imago of the object-glass
would be formed by it A "stoii" or di.iphi-agm CB must Im
placed between tlio two lenses, is the visual focus of tlio eye-glass,
which is, of course, the position wherein tlic image of tho object
M'ill bo formed by tlie rays brought into convergence by their
[.assago through the field-glass. Huygens devised this airaiig*-
ment meicly to diminish the s|dicncal aberration ; but it was subse-
quently shown by Uoscovieh tliat tho chromatic dispeisioit was al.^o
ingieat part collected by it. Since tlio iiitroductiou of achromatic
object-glasses for coni[iound microsco)»es, it has been further ftliovvii
be avoided by a slight over-con-cction o(
id red rays may be daused to ciitcj- the
eyo in a paiallel diiecliou (though not actually coincident), and
thus to proiluco a colourless imnge. Tlaislct N, !M. N (fig. 14) i-cpro-
sent tlio two extremo ravs of threo j»encils, which without tho
field-glass would form a blue image com'cx to the eve-glass at Cl>,
and a red one at RR ; then, by the iiitervelitioM of 'ihc field-glass,
a bltru imago concavo to the eye-glass is formed at B'C, and a led
* Thus it is dtill a moot point whether tho niicro5Coi»ic appear-
ances seen in tho siliceous valves of diatoms (tigs. 8-11) are th<
optical repre-senlalioiis of elevations, depressions, or perforations, or
of internal nielecular arraugeuieuts not iuvoh ing any iucquaJity oi
surface.
* This doctrine was fii-st fully develo]l«ll by Professor Abbo in the
Archil' fir Murosi. .ImilcMie, vol. ix. (1874), nnd is nioro lully »i-
poundetl in his ^ub^elplent contributiolis to Jour. Roij. Micros. &>fc'
^ee also tho papeii of Mr Slepheiisou and Mr Crisp iu tlmt journal,!
ami In tho preccling Muuthhj Mii-i'r.scnj'iciil Joiiniat.
* Any good worknmn can now make by tho dozen such snioll-Qiigled
J inch objectives as Jlr A. Uo.« prodiicoil with inucU poins and luUonr
lifty ycain ago. it was not until 184 4 tlmt, wiih tho honomabU
eniulutiou of Burp.nssing what Piofesior Aniici b.id then accon>pUili«d^
lit produceil a .,V, inch of 133°, which, by taking ailvantnga of fptyl
voiy heavy fliiit*gla^ ko bad, he afterwards increased to 170*-'
MICROSCOPE
2G7
one at ETI'.^'As the foctu of the eye-gUss U shorter for blue laya
th»n for red rays by just the difference ia the pUce of these im&^,
their rays, after refraction by it, enter the eye in a parallel direction,
«nd produce a picture free from^ £al3e_ colour. j«If the object-glasa
had been Tendered perfectly ' ^^^^^^^^^^^^^^^^^^^
achromatic, the blue rays,
after passing through the
field-glass, would have been
brought to a focus at b, and
the red at r ; so that an error
Ktmld be produced, which
Tfonld hare been increased in-
stead of being corrected by the
eye-glass. Another advantage
of a weU-constmcted Huy-
ffunian eye-piece is that the
unage produced by the meet-
iqg of the rays after passing
through the field-glass Is by it
rendered concave towards the
■eye-glass instead of couvc-a,
JO that every part of it may
.be in focus at the same cime,
«nd the field of view thereby
Tendered flat'
^ TwoormoreHuvgenianeye-- ,, „ .. , ti t,
xng powers, known as A B, C jjicriscopic Objectives.
«c., are usually supplied with "^
a compound microscope. The utility of the higher powers will
mainly depend upon the excellence of the objectives ; for, when an
achromatic combination of small aperture which is sufficientlv well
corrected to perform verj* tolerably with a *'low" or "shallow"
eye-piece is u*ed with an eye-piece of higher ma|^if)-ing power (com-
monly spoken of as a *' deeper " one', the image may lose more in
Inightness and in definition tnan is gained by its amplification, while
"tile image given by an objective of large angular ai>erture and very
f effect correction shall sustain so little loss of light or of definition
y "deep eye-piecing " that the increase of magnifying power shall
he almost clear gain. Hence the modes iu wliich different objectives
of the same power, whose performance with shallow eye-pieces is
nearly the same, are respectively affected by deep eye-pieces afford
a good test of their respective merits, since any defect in the correc-
tions is sure to be brought out by the higher amplification of the
image, while a deficiency of aperture is manifested by the want of
light. The workin" microscopist will generally fin'l the A eye-
piece most suitable, D being occasionally employeil when a greater
power is required to separate details, whilst C anil others still deeper
are useful for the purpose of tasting the goodness of objectives, or
for special investigations renuiring the highest amplification with
objectives of the finest quality. But he can commit no greater
■error than habitually to use deep eye-pieces for the purposes of
scientific research, especially when (as in the study of living
objects) long-continued and unintemiitted ohsen-ation is necessarj-.
For the visual strain thus occasioned is exactly like that resulting
from the habitual use of magnifying spectacles in reading, requir-
ing the book to be held within 2 or 3 inches of the eye. And
«ll experience shows tliat this feeling of strain cannot be dis-
TC^rded, without the most injurious consequences to ^nsion.
♦ Tor viewing large flat objects, such as transverse sections of wood
■or of ^cAi'nru spines, under low niagnifpng powers, the eye-piece
'known as Kelliicr's mav be employed with advantage. In this
construction the field-g^ass, which is a double-convex lens, is
5 laced in the focus of the eye-glass, without the interposition of a
iaphragm ; and the eye-glass is an achromatic combination of a
plano-concave of flint with a double-convex of crown, which is
•lightly under-corrected, so as to neutralize the over-correction
given to the objectives for use with Huygenian eye-pieces. A
flit well-illuraiuited .field of as much as 14 inches in diameter
may thus be obtaincd''with .very little loss of light ; but, on the
other hand, there is a certain imi>airmeiit of defining power, which
renders the Kelliier 'eye-piece unsuitable for objects presenting
minute structural details ; and it is an adJitional objection that
tlie smallest speck or amear uiwn the surface of the field-glass is
made so unpleasantly obvious that the most careful cleansing of
that surface is reljiiired every time that tliis eye-jilece is used.
Hence it is better fitted for the occasional display of objects of the
character already specified than for the ordinary wants of the
.Trtrking microscopist.
6olid eve-pieces, consisting of cylinders of glass with convex ends,
*r» sometimes used in place of the Huygenian, when high magni-
ftTnjrpowcr is i-equircd for testing the i»erformance of objectives.
■Theiowcr surface, which has the lessor convctitv, serves as a
I'Tlic renter m\y be referred to Mr Vtrley's inrcati^tioa of the properties of
<lw HujrfWiiUn cyc-piecc la tlic flfty-Rnt volotrc of the TrafiiaclioMM of tht
■Sottttg •/ Artt\ Bad to the ■rticle •' Microscope." bv >lr Unas, In the A«J»J'
4)itltfKii^ ttpriue<l, irUh ailOitiuiu. In the iTaiVu* Citlap*/''
field-glassL while the image formed by this is magnified by the
highly convex upper snrface to whicn the eye is applied, — the
advantage derivable from this constmction lying in the abolition of
the plane surfaces of the two lenses cf the ordinarv eye-piece.' v
A " positive " or Bamsden's eye-piece — in which the field-glass,
whose convex side is turned npwarus, b placed so much nearer the
eye-glass that the image formed by the objective lies below instead
of above it — was formerly used for the purpose of micrometry, — a
divided glass being fitted in the exact plane occupied by the image,
so that Its scale and that image are both magnified together by uie
lenses interposed between them and the eye. The same end, how-
ever, may be so readily attained with the Huy^nian eye-piec«
that no essential advantage is gained by the use of uat of Bamsden.
the field of which is distinct only in its centre.
Objectites.
It has been seen that one of the principal points in the con-
struction of microscopic objectives to which the attention of their
makers has been constantly directed has been the enlargement
of their " aperture," — this term being understood to mean, not
their absolute opening as expressed by linear measure, but their
caj«city for receiving and bringing to a remote conjugate focus the
raj's diverging from the several points of a near object. The aper-
tnJe of au o^'ective has been usually estimated by its "angle of
aperture, " — that is, by the dcOTee of divergence of the most extreme
rays proceeding from the axial point of the object to the margin of
the objective (fig. 15) which take part in the formation of the
image. It is pointed out, however,
by Professor Abbe that, in the case
of single lenses used as objectives,
their apertures are really propor-
tional, not to' their respective angles
of aperture, but to the ratio between
the actual diameter or clear opening
of each to its focal distance, a ratio
which is simply expressed by the
sine of its semiangle. And in the
case of combinations of lenses it can
be demonstrated mathematically that
their respective apertures are de-
terminable— other conditions being
the same — by the ratio of tlie dia-
meters of their back lenses, so far as Fic. 15. — Section of Achromatic'
these are really utilized, to their Object-Glass, composed of
respective focal lengths,— this ratio thiee pairs of (nint and
being expressed, as before, by the sine "O'™) lenses, oic is its angle
of the semiangle of aperture (sin u). of aperture.
The difference between these two modes of comparison can be
readily made obvious by reference to the theoretical maximum of
180°, which is attained by opening out the boundaries of the angle
abc (fig. 15) until they come into uie same straight line, the sine cf
the semiangle (»0°) then becoming unity. For, while an objective
having an angle of 60° would count by comparison of angles sa
having only one-third of the theoretical maximum, its real aperture
would be naif that maximum since the sine of its semiangle
(30°) = i. And, as the sines of angles beyond 60° increase very
slowly, an objective of 120° angle will have as much as 87 per cent
of the theoretical maximum of aperture, although its angle is only
two-tliirds, or 66'6 per cent, ol^ 180°. It hence becomes obrious
that little is really gained in real aperture by the opening-out of
the angle of microscopic objectives to its greatest practicable limit
(which may be taken as 170°), while such extension — even if
unattended with any loss either of definition or^of colour-correction
— necessarily involves a great reduction alike hi the working dis-
tance and in the focal depth or penetration of the combination,
as will be presently explained.
Xumerieal Aperture. — It hasnowbeen demonstrated by Professor
Abbe that,. independently of the advantages already specified as
derivable from the application of the immersion sj'stem to objectives
of short focus and wide aperture, the real aperture of an immer-
sion objective is considerably greater than that of a dry or air
objective of the same angle, — the comparative apertures of objec-
tives working through different media being in the compound
ratio of two factors, viz., the sines of their respective seoiiangles
of aperture and tlie refractive imUces of the "immersion" fluids.
It is the product of these (jisinii) that gives what is termed by
Professor Abbe the "numerical aperture,' .—which serves, therefore,
as the only true standard of comparison, not only betvveen dry_ or
air and water or oil immersion lenses, but also between immersion
lenses adaptetl to work respectively with water, oil, or any other
interpiKed fluid. Tliat the angle' of aperture eipre.«ed by the
same number of degrees must correspond with very different work-
ing apertures in dry, water immersion, and oil or homogeneous
immersion objectives becomes evident when we consider what
268
MICROSCOPE
happens when divergent pencils of rays pass from one medium
into another of hi*;hcr refractive index. For such diver/^'ent
pencils, proceeding from air into water or oil, will be closed
together or compressed ; so that the rays which, when an object
is mounted in air, spread out over the whole hemisphere then
form comparatively narrow pencils, and can thus be utilized
by an immersion objective of smaller aperture than is required in
a dry objective to admit the most diverging rays of air-pencils.
It follows, therefore, that a given angle in a water or oil immersion
objective represents a much larger aperture than docs tlie same
angle in an air-objective ; and tlius it comes to pass tha* by
openiufT out the angle of immersion objectives they may be made
to receive and utilize rays of much greater divergence than can
possibly enter dry objectives of even maximum aperture.
The following table, abridged from that given ny Professor Abbe
for every 0*02 of numerical aperture from 0*50 up to the maximum
of l"f2, brings this contrast into clear view : —
Niimcrical Apcrlurc Table.
An
glc of Apcit
rrc (=:«).
lUumi-
Tlteoreliciil
Resolving
1
Penc-
Numcncfll
Power, in
traliiiB
Aperture
Drj
Watcr-
HomoRcncous-
natinfi
Power
Lines to
Power
(nsinu=a).
Objec-
tives
Immer^ion
Objcclives
Immcisiion
Objectives
an Ineli
(i=0-62C9^
(!)
("=I).
(,1=133).
(n=l-52).
=line E).
1-52
ISO 0
2-310
140.628
-656
1-12
138 12
2-016
136,S83
-704
1-33
isb" 0
122 6
i-7:o
128,212
■762
1-26
142 30
111 69
1-683
121,404
-794
lis
125 3
101 60
l-3r2
11:!,7.'.2
-847
112
114 44
94 66
1-254
107.908
-803
1-06
105 42
68 20
1124
102,184
■943
1-00
180" 0
97 31
62 17
1000
96,400
1000
0-94
HO 6
89 66
70 24
■SS4
90,010
1004
0'S6
113 38
80 34
68 64
■740
8',904
1103
0-80
lOG 16
73 68
63 31
•040
77,120
1260
0-7C
38 SO
69 42
60 0
-573
73,2'.l
1-310
0-70
88 51
03 31
64 6J
•490
07,480
1-429
0-62
70 38
6ii 34
48 9
•384
69,708
1013
0-56
08 6
40 48
43 14
-314
63,984
1-7S0
0-50
00 0
44 10
38 24
•260
48,200
2000
Thus, taking .is a standard of comparison a dry objective of
the maximum theoretical angle of 180°, whose numerical aper-
ture i^ the sine of 90°, or 1-00, we find this standard equalled
by a water-immersion objective whose angle of aperture is no more
than 97^°, and by an oil or hon ogoneous immersion objective
of only 82°, — the numerical apertures of these, obtained by multi-
plying the sines of their respective semian'gles by the refractive
index of water or of oil, being 1-00 in each case. Each, there-
fore, will have as great a power of i jccivin§ and utilizing divergent
rays as any dry objective can even theoretically possess.
But, as the actual angle of either a w-ater or an oil immersion
objective can be opened out to the same extent as that of an air or
dry objective, it follows that the ajierturc of the former can be
augmented far beyond even the thi^oretical maximum of the latter.
Thus the numerical aperture of a water-immersion lens of the
maximum angle of 180° is 1-33, or one-third greater than that
of an air-lens of the same angle ; and this apertiu-e would be
given by an oil-immersion objective of only 122°. Again, tho
numerical aperture of an oil-immersion objective having the theo-
retical maximum angle of 180° would be 1-52, or more than one-
half greater than that of an air-lcus of the same angle. And the
numerical apertures corresponding to angles of 170, which have
been actually attained in both cases, fall very little short of the
proportions just given.
So, again, an oil-immersion objective whose angle of aperture is
only 60° has as high a numerical aperture (0'76) as a water-
immersion objective of 69i°, or as a dry objective of 99°; and a dry
objective of 140° has no greater a numerical aperture (0'94) than
a water-immersion of 90° or an oil-ii.imersion of 76 J°.
This important doctrine may be best made practically intelligible
by a comparison of the relative di.-.metcrs of tho back lenses of
dry with those of water and oil immersion objectives of the
same power, from an "air-angle" of 60° to an "oil-angle" of
180°, — these diameters expressing, in oach case, the opening between
the extreme pencil^forming rays at their issue from the posterior
surface of the combination, to meet in its conjugate focus for tho
formation of the imajo, tlie relation of which opening in each case
to the focal length of the combination is the real measure of its
aperture (fig. 16). Thus the dry objective of 60° angle (5 in fig. 16)
has its air-angle represented by sin ti — J -0-50 numerical aperture.
The dry objective of 97° (4) has its air-anglo renrcsenttd by sinu-
3 -=0-75 numerical aperture. And the dry objective having the
(theoretical) angle of 180° (3) has its air-angle represented bysinii
— I'OO numerical aperture,— this corresponding to 96° water-
angle and 82° oil-angle. But tho water-immersion lens having
the (theoretical) angle of 180° (2) haa its watcr-aiiglo represented
b; nsinu — 1'33 Jiumerical aperture. And the oil-inunersion
lens bavin" tho (theoretical) angle of 160°^(I) has its oil-anglo
rcprosentciT by nsinit — 1'52 "numerical aperture."' Theso
theoretical apertures for water and oil immersion lenses having been
found as nearly attainable in practice as the theoretical maximum
for dry objectives, such lenses can utilize rays from objects
mounted in balsam or other dense media,
which arc entirely lost for the image (sinci-
they do not exist physically) when the sam<-
object is in air or is observed through a filni
of air. And this loss caimot be compcnsatcil
by an increase of illumination ; because thi-
rays which are lost are different rays physi-
cally from those obtained by any illumi-
nation, ho)vover intense, through an aeriform
medium.
It is by increasing the number of diffrac
tion-spectra that the additional rays thuv
received by objectives of great numerical
aperture impart to them an increased resolv-
ing power for lined and dotted objects,—
the truth of the image formed by the recom-
bination of these spectra being (as alread\
shown) essentially dependent on tlic minibci
of thein that the objective may be capable
of receiving.
But whilst the resolving power of micro
scopic objectives increases in the ratio ol
their respective numerical apertures, and
whilst their illuminating power (dependent
upon the quantity of light that passes
through them) increases w-ith tlie square of
the numerical aperture, ihe case is reversed
with another most important quality, — that
of penetration or focal depth ; "for this
diminishes as the numerical aperture in-
creases, until notliing but what is precisely
in the focal plane can be even discerned with
objectives possessed of the highest resolving
power. Thus, tho pchctrating power of an Fig. 10.— Uilative Di.i-
objective of 60° air-angle being expressed meters of Back Lenses
as 2 000, an extension of that angle to 76i° of Air, Water, and
reduces it to 1-613, an extension to 89° 9" Immersion Objec- ,
reduces it to r429, and an extension to 99° *'"^''
reduces it to 1-316; further extension to 118J° reduces it to 1-163,
w-hile an objective whose air-angle is 140° has a penetrating power
of only 1 064. So, again, the oil-immersion objective wliich h.as the
numerical aperture of 1-00 corresponding to the theoretical air-
angle of 180° has a penetrating power of I'OOO; this is brought
down to '752 when its angle is so increased as to make its numerical
aperture 133, equalling the theoretical maximum of a water-
immersion objective, and is '658 at the theoretical maximum (1 ■52>
of an oil-objective.
Hence it is clear that, as some of the qualities to be sought ii:
microscopic objectives are absolutely incompatible, a preference is
to be accorded to objectives of greatest resolving power but very
little penetration, or to those of moderate resolving power and
great penetration, according to the uses to which they are to be
applied; and some general principles will now be laid down in
regard to this matter, based alike on science and experience.
In the first place, a marked distinction is to be drawn between
those objectives of low or moderate power which arc tp be worked
dioptrically and those of high power which are to be worked dif-
fractivcly. The objects on which the former arc to be for the most
part used are either minute transparent bodies having .solid forma
which the observer should bo able to take in as wholes (as in the
case of Pohjcysiina, the larger diatoms, /ii/usoria, kc); or trans-
parent sections, dissections, or injections, whose parta lit! in
different planes, the general relations of which he ilesii-es to study,
while reserving their details for more special scrutiny ; or opaque
objects, whoso structure can only be apprehended from the
examination of their surfaces, wiien the inetjualities of those sur-
faces arc seen in their relations to each other. In all these cases
it is desirable that microscopic vision should resemble ordinary
vision as much as possible. If the eye were so constructed as to
enable us to discern only those parts of an object that lie pre-
cisely in the plane to w-hich wo focus it, our visual conceptions of
the forms and relations of these parts, and consequently of tho
object as a whole, w-ould in general be very inadequate, and often
erroneous. It is because, w-hile focussing our eye successively on
the several planes of the object, w-e can see the relation of each to
what is nearer and moi-o remote that w-e can readily acquire a
visual conception of its shape as a whole, and that unmistakablo
perception of solid form which is given by the combination of the
two dissimilar perspectives of near objects in binocular vision
» The (lotted clreles In tlw? interior of 1 nnd 2. of the same diameter as 3, show
the cxeess In the dlnmetcrs of the back lenses of tho water and oil objectlre*
over Uiat of the dry at tudr rc-^ectlvc thcoretlcnl Ilml(«.
MICROSCOPE
2G0
r^ 9?'«^-«.nH ^5t riSblTbTfomed if our Tision were strictly i each pair. When, on the other hand it is desired to scnitinize mth
(p. 273) could °»\P^f'°7 °V; 'r„,,,. ._.„ .„ focusscd the greatest precU on such minute details as are presented in one
b'mited to the exact plan^ or which ou.e ^^^S'^^^^ ^^J ^^^j ^^^ ^^^J^^ the thinnest
Hence it is obvious that, in rnc case oi "oji^"'' "."''" ..,.^.. _.„:v,u ci™ „f »;„„,„ o„,.„„,i „„f K.f„,»„ a „1a« sliHn am its cover-
Hence It •^°»!X^''^'','",'"h oV penetraton is a quality possible film of tissue spread out between a glass slide and its cover-
niodemte »™Pl'h<=»t'°r>,/™^' ^.'P*''„°; ,r"7^^^^^^ 1 fng glass), the microscopist wUl prefer an objective in which focal
Se 'X'S°ou"t oftheir^^p^rtu" s'^elng 0^1^ adTaZg^^^^^^ de|t1i is'subordinated 'to aperture, for the ike of the. resolving
so far as it does not seriously interfere with their penetrating
Bower It is, no doubt, quite possible to construct a 1 inch
obiective with an aperture so large that, when the requisite ampU-
fication has been gained by deep eye-piecmg, it shall resolve
the lined "tests" ordinarily used for a i, or to construct ^an
objective of tV i°<:h focus which shall in like
ordinary work^f a J. But, as such objectives "
thi
^ _^ thereby spoiled
for their own proper work, the loss to the microscopist is but
noorlv compensated by his ability to resolve with them, under such
deep eye-pieces as cannot be habituaUy used without scnous risk to
the eye-sight, the lined and dotted tests which can be much better
shown under objectives of shorter focus and wider aperture, with eye-
pieces of low amplification. For, whUst deep eye-pieces cannot bo
Bahitually employed for continuous observation, without putting
a strain upon the eyes resembling that which results from the
constant use of a magnif5-ing glass, even the very highest objectives
may be used continuously for long periods in combinaUon with
shallow eye-pieces, with scarcely any fatigue, and therefore (it is
probable) without sensible injury.i .
In estimating the goodness of a microscopic objective, five
distinct qualities have to be separately considered:— (1) 1*3 work-
in)? dUtance, or the actual interval between its front lens and the
object on which it is focussed; (2) its penetrating power, or focal
depth; (3) the flatness of its field; (4) its definition, or power ot
mnn" a distinct image of all well-marked features of an object,
and Specially of their boundary lines; and (5) its resolving pon-er,
by which it separates closely approximated lines, dots, or striK.
1 The " working distance " of an objective has no fixed relation
to its focal length,— the latter being estimated by its equality in
»awer with a single lens of given radius of curvahire (such as
1 inch, J inch, -^ inch, &c.), while the former varies with
the mode in which the combination is consti:ucted and with the
aperture given to it. For low and moderate powers, ranging up to
■X, inch focus, good working distance is especially important,
alike bocause it is closely related to penetrating power, and also
because it facilitates the use of side-illumination for opaque objecfa.
And in such objectives of high power as are to be used, not for the
resolution of lined or dotted tests, but for the observation of living
and moving objects ot extreme minuteness, good working distance
is no less important, on account of its relation to focal depth. In
the case of those objectives, on the other hand, in which resolving
power is made the first consideration, it is only needful that the
working distance shall be such as to peimit tlie inteiiiosition of a
thin glass cover ; and this, although necessarily diminished with
the n-idening of the aperture, can be always obtained by the adoption
of the immersion system.
2. The " penetrating power" or "focal depth" of an objective
may be defined as consisting in the vertical range through which
the parts of an object not precisclv in the focal plane may bo so<?i
with sufficient distinctness to enable their relations with what lies
exactly in that plane to be clearly traced out,— just as would be done
by ordinary vision if the object were itself enlarged to the dimen-
sions of its microscopic image. The dose relation between this
quality and the preceding becomes obvious when it is considered
that the longer the working distance of an objective the less will
the distinctness ot the imago it forms be adected by auy given
alteration (say the ttj^tj of an inch) in its focal adjustment. Con-
sequently, of two objectives having the same magnifying power but
different working distances, that one will have the most focal ilepth
whose working distance is the gicater. On the other hand, as the
penotiating power of an objective is reduced in direct accordance
with the increase of its numerical aperture, it must be san-ificed
wherever the highest resolving power is to be attained. Hence,
as already remarked, this attribute will be very differently valued
by different observers, according to the work on which they are
rcsi<ctively engaged. For the general purposes of biological
research, not only with low or moderate (tor the reasons already
stated , but also with high powei-s, a considerable amount of
focal depth is essential. It is impo.saible, for example, to follow
satisfactorily tlio movements of an Ama-bn, or to study the
"cjclosis" in the cell of a ValUsnn-ia, or to ti-ace iho dl>>tribution
of a nerve-tlireail, with an objective in which focal depth is so
comjiletely sacrificed to aperture that nothing can bo dibcerued
save what is precisely in the focal jilane, since, iu-tcad of parsing
gradalionally from one focal jdane to another, as the ob.-er\cr can
9 do with an objcttivc of good iienetration. he can only get a succes-
sion of "dissolving views," with an interval of "tliaos" between
1 III nco. for woik of this kin I. Iho »hnlh>»c' eye pl.co« an.l h.nccr lulies ut
English itiirroscopes are to beprcfetred tollic ilccpciH-j -vh CfsantI shoil-rtiibc^
ot ti.corJIniuyConlincnlal nioilvl. tlic sliallowcst i.'y>.-l.li-ccj of the liillcr being
usoAUy equal iu po^^er to the oidinury B i>c-idecc& uf the (oiincr.
depth is subordinated to aperture,
power which he can thus command. And it will often happen in
biological research that it is advantageous thus to bring objectives
of the latter class to bear upon objects whidi could not have been
detected in the first instance save by objectives of much inferior
resolving power but greater focal depth.
3. The "flatness of the field" afforded by tlio objective is a
condition of great importance to the advantageous use of the micro-
scope, since tiio extent of the area clearly seen at one time procti-
cally depends upon it. Slany objectives are so constinicted that,
even wheu the object is perfectly flat, the foci of the cential and
peripheral parts of the field are so different that, when the adjust-
ment is made for one, the other is more or less indistinct. Hence,
when the central part of the area is in focus, no more iuformation
is gained respecting the peripheral than if tiie latter had been alto-
gether stopped out With a really good objective, not only shoidd
the imago be distinct over the whole field at once, but the marginal
portion should be as free from colour as the cential. As inipcifec-
tion in this respect is often masked by the contraction of the
aperture of the diaphragm in Oie eye-piece, the relative meiits of
two objectives, as regards flatness of field, should always be tested
under an eye- piece giving a large aperture.
i. The "defining power" of an objective, which depends upon
the completeness of its corrections for spherical and for chromatic
aberration, and upon tlie accurate centring of its component lenses,
is au attribute essential to its satisfactory performance, whaUvor may
be its other qualities,— its importance in scientific reseanh being
such that no superiority in resolving power can compensate for the
want of it; aT\d, though it is possible to obtain perfect con-ection for
siiherical aberration up to the liighest practicable limit of angle, yet
the difficulty of securing it increases rapidly witii tho augmenUtion
of aperture, the want of it being made perceptible, especially when
deep eye-pieces are put on, by the blurring of clearly-marked lines
or edges, and by general "fog." Perfect colour-con-ection, on the
other°hand, is not possible for dry lenses ot the widest angle, on
account of tho irrationality of the secondary specti-um ; but this
may be neuhalized by tlio use of the immersion system. As already
sUted, what has to be aimed at in the coustiuction of microscopic
objectives is not absolute colour-correction, but a slight degi-ee_ of
over-correction, which, by compensating the chromatic dispereiou
of the Huygenian eye-piece, shall produce an image fi-ee from false
colour. As this can be secured far more easily in the constiucfaon
of objectives of moderate than in those of very w4de aperture, tho
cost of tho former is proportionally small,— au additional reason
for the preferojice to bo given to tiiem on other grounds, iu regard
to all save very special kinds of microscopic work.
5. "Resolving power, ' being that by which very minute and
closely approximated markings— whether lines, shrise, dots, or
aperhires— can be separately discerned, is a function which is only of
primary importance in objectives whose amplifying power siiecially
fits them for the study of objects of this class. It appears from the
matliematical researches of Professor Abbe that the maximum
resoU-ing power (with a theoretical angle of 180°) would be capable
of separating 1-16,528 lines to the inch ; but he considers the limit
of visual resolution depending on the power of the eye to be about
-PPiVtre of an inch ; and this limit seems to have been nearly
reached. To make such a separation distiuctly perceptible, an
amplification of at least 3000 linear would be requisite; and this
can only be obtained citiier by the use of an objective of very high
power (such as -^ inch focusl in combination witli a low or nieduini
3S-e-piece or by'putting a very deep eye-piece upon an objective of
lower power (such as a i inchl,— the former method, for tlie reasons
already given, being ilecidedly preferable. For the resolution of less
closely appro.'iimated markings objectives of -^t Ai i*?- *'"J »
inch answer very well ; and the resolving power which they
require niav bo obtained witiiout any excessive widening of the
aperture. Vor tiie loss of resolving power consequent upon the
contraction of tlie angle of a walei-inimci-sion objective to 128J is
only oue-tentli of tlie'thcoreti^al maximum 128,212 ; while a reduc-
tion to 1055° only lowers tlie number of separable lines to 102,184
to the inch.— tints diminishing the resohiiig power by little mote
titan one-fifth, while tho working distance ami focal depth of the
combination are greatly increased, and perfect defimrion is moro
certainly attahiable. The i inch is (according to the writers
experience, whicli is coiifirmcl bv tiie tlieoretical deductions ol
Professor Abbe) tho lowest objective in whidi resolving powei
should be made the primaiT qualification,— tiie J, J, },; anil , J
inch belli" specially suited to kinds of biological work in \yhicli
this is fai°les3 important than focal deptii and dioptric precision.
This view is strengthened by tiie very imj-ortant consideration that
tho rcsolvin" power given bv wide apertiiie cannot be utiltzed,
I e.'ccept by a nioihod of Uluin-uation that causes light to pasa thiougH
270
MICRO SCO P E'
the object at iin oHiquity coh'csponding to that at which tlie most
(livci-gcnt rays enter the objective. Now, althou"li in the case of
object* whoso markings aic only superficial siicli obliiniity may not
bo proiUictivo of false appearances (though even this is scarcely con-
ceivable), it must have tliat effect when the object is thick enough
to have an internal structure ; and the experience of all biological
observei-s who have carried out the most delicate and dilHcidt
investigations is in accord, not only as to the advantage of direct
illumination, but as to the deceptivcncss of the appearances given
by oblicpie, and the consequent danger of error in any inferences
drawn from the latter. Thus, for example, the' admirable researches
'of Strasshur^er, Fleming, Kh'in, and others upon the changes whicli
take place in cell-nuclei during their subdivision can only be
followed and verified (as the writer can personally testify) by
examination of these objects under a.xial illumination, with objec-
tives of an angle so moderate as to possess focal depth enough to
follow the wonderful did'ercntiation of component parts brought out
by staining processes througli their whole thickness.
The most perfect objectives for the ordinary purposes of scientific
research, therefore, will be obviously those whicli combine exact
definition and flatness of field with tlie widest aperture that can be
given witho\it an inconvenient reduction of working distance and
loss of the degree of focal depth suitable to the work on which they
are respectively to be employed. These last attributes are especially
needed in the study of living and moving objects ; and, in the case
of these, dry objettives are decidedly preferable to immersion,
since the shifting of the slide which is requisite to enable the move-
ment of the object to bo followed is very apt to produce disarrange-
ment of the interposed drop. And, owing to the solvent power whfch
the essential oils employed for homogeneous immersion have for
the ordinary cements and varnishes, such care is necessary in the
use of objectives constructed to work with them as can only be
given when the observer desires to make a very minute aud critical
examination of a securely-mounted object.
The following table expresses the magnifying powers of objectives
constructed on the English scale of inches and parts of an inch, with
the 10 inch body and the A and B cye-picccs usually supplied by
English makers, and also specifies the angle of apertutc which, in the
\vriter's judgment, is most suitable for each. He has the satisfac-
tion of finding that his opinions on tliis latter point, which are
based on long experience in the microscopic studv of a wider range
of animal and vegetable objects than has fallen within the purview
of most of his contemporaries, are in accordance with the conclu-
sions drawn by Professor Abbe from his profound investigations into
tho theory of microscopic -vision,' whicli have been carried into
practical accomplishment in the excellent productions of Mr Zeiss.
Maun
(jlng
Slncr,
fylng
Focnl
length.
Angiilfir
Aperture.
cr.
FoMl
Length.
AiifTular
Al.crlure.
cr.
A Eye-
B Evc-
A Eye-
B Evc-
^
piece.
plecc.
piece.
plccc. 1
4 rhclies
;
12
18
i Inch.
50-80
ioo
12
18
27
95
2-.0
15
ti
87
1 <
110
V "
20
30
it
9 ,.
1-10
400 •
CO
T'.
A ■..
150
500
1 .,
40
-5
112
\ ..
1(10
GOO
1 "
44
100
1.50
s .
170
800
A n
125
187
. For ordinary biological work, the J, yVt and jJ, objectives, with
aiiglea of from 100° to 120°, will be found to answer extremely
well if constructed on the water-immersion system.
-Each of these jiowers should bo tested upon objects most suited
Hrdctcrmiue its capacity for the particular kind of work on whicli it
i» to be employed; and, in such testing, the application of deepeioye-
piecea than can be habitually employed with advant.ige will often
serve to bring out marked diiferenccs between two obje'c-tivcs which
seem to work almost equally well under tliose or.linarily uscil,—
defects in definition or colour-correction, nud want of light, which
■Bight otherwise have escaped notice, being thus niado^apparent.
No single object is of such general utility for these purposes as a
large well-marked PoiUira scale ; for the eye which has been trained
to the use of a particular specimen ol it w ill soon loam to rccogiii«
by its means th/j qualities of any objective lictwccn 1 inch and f
inch focus ; and it may bo safely asserted that the objective which
most clearly and sharply exhibits its chaiacteristic markings is the
best for the ordinary work of the histologist.
For the special attribute of resolving power, on the other hand,
tests of an entirely dilfcrent order are required ; and tliese are fur-
nished, as already stated, cither by the more "dilficnlt" diatoms,
or by the highest numbers of S'obert's ruled tcstplatc. Tlie
diatom-valve at present most in use as a test for resolving
power is the Amp/iiplcitra pclliici'Ut, the lines on which were long
supposed to be more closely ap]iroxiniatcd than those of Koberts
nincteentli band, being affirmed by Mr SoUitt to range from 120
to lyo in riVi! of an ineli. But'the admirable photographs of
this valve obtained by Colonel Dr ^Voodward have confirmed the
conclusion long previously expressed by the writer, that this esfi'-
mate was far too high, being based on the "spurious lineation'i
juoduced by dilfraction, and show that the strioe on the largest
valves do not exceed 91, while those on the smallest are never more
numerous than 100, in „Vir of an inch. The same admirable
manipulator has also obtained excellent photographs of another very
difficult test-diatom, Siirirclla gcmmn, from which it appears
that its transverse stiia; count longitudinally at the rate of 72,000
to the inch, whilst the beaded appearances into which these may
be resolved count transversely at tlie rate of 84,000 to the inchj
Thus it aiipears that the complete resolution of these "vesatiousij
diatoms dors not require by any means the maximum of aperture'
but is probably dependent at least as much on the perfection of the
corrections and the elfcctiveness of tlie illumination.
It must be understood that there is no intention in these remarks
to undervalue the efforts which have been pcrseveringlv made byi
the ablest oonBtruetors of microscopic' objectives in the <{irection of
enlargement of aperture. For these efforts, besides increasing the'
resolving power of tho instrument, have done tlie great service of
producing a vast improvement in the quality of those objectives of
moderate aperture which are most valuable to the scientific biolo-
gist ; and the microscopist who wishes his aiinamcntum to be com-'
plete Will provide himself witli objectives of those difl'erent qualities,^
as well as different powers, which shall best suit his particul%5
requirements.' -
iLLUMrXATIXO ApPARATTS.
Every improvement in the optical performance of the compound
achrotnatic microscope has called forth a corresponding improve-j
ment in the illumination of the objects viewed by it, since it soon
came to be anparent that without such improvement the full ad-
vantage of the increased defining and resolving powers of th^
objectives could not be obtained. For the illumination of trans^
parent objects examined by light transmitted through them unde^
low powers of moilerate angle a converging pencil of .rays reflected)
upon their under surface by a concave mirror is generally sunicient,-3
a "condenser" being only needed when the imperfect trausparenc*
of the object requires the transmission of more light through iq
And the microscopist engaged in ordinary biological studies, who
works on very transparent objects with objectives of J or J incti
focus, or t", inch immersion, will find that tho small concaW
mirror of short focus with which the Continental models are fur^
nished (sec fig. 28) will generally prove sufhcient for his needs. Thi)
mirror is nsually hnng at snch a distanc* beneath the stage ^hai
parallel rays falling on it are brought to a focus in the (^jject as it
lies on a slip of glass resting on the stage ; an.l thus, when the
instrument is used by day, the light of a bright cloud (which isprej
fcrable to any other) gives a weil-iHuminatcd field, even with thi
powers last-mentioned. But when laniidight is used its divergent
rays are .-lot brought to a focus in the object by a mirror that iJ
fixed as just stated; and the distance of the mirror bcneatli the
stage should be made capable of increase (which is easilv done bj
attaching it to a lengthening bari, so as to obtain the requisite
focal convergence. Still the best ell'ccts. of objectives of less than
i inch focus cannot bo secured without the ai.l of an achromatic
condenser, interposed between the mirror and the object, so as to
bring a larger body of rays to a more exact convergence.
When objectives of stiil higher jiower are employed, fhe employ-
ment of such a condenser becomes iiidisiiensable ; and when thp
lii,i;lie-.t powers are being iiscil by lamplight, it is desirable to dis-
jii'iisc with (lie mirror altogether, and loplacc the flame exactly in'
tlio optic axis of the microscope. Tlie condenser shoul.l be an
a'iiroinatic cnmbiiiation, corrected for the ordinary thickness of
till) glass sli|i on which the object li-.-s, and capable of being so
adjusted as to focus the illuiiiinatiug pencil in the object.'
As it is often foun.l desirable that an object slionld bc"illuniinated
by centra! rnvs alone, or that the qnantitv of light transmitted
through it should be reduced (for bringing into view delicate dctaiU
of structure whicli are invisible when the object is flooiloJ nith'
light), every microscope should bo provide.! wiili some means oi
cutting olV the oul.-r rays of t!ic illuniinaliiig cone. T!ie "ilia?
phi.agin-plate" or.linarily nsc.l for this pur|>OH' is a disk of blaelc
Mietal. i.ivotcdto tlienn.lcr si.le of the stage, an.l perforated witlii
gra.liiate.Isoriesofaprrluresof dilfircnt.liaiiietei-s, any one of wliicK
can bo brought, by the rotation of the di^k, exactly into the o|itic
axis of the microscope. But the rci|uired elfcct caii bo much more
advantageously obtained by the " iiis.liaphraguf,"* in which a
niiinbir of c.mvergiiig plates of metal are made so to sli.lc'over
each other by the motion of a I. ver or screw . thatl|ithe'-'a|yr^
tuiv is either enlarged or diminished, while alw.aysieniainiiig-'pi-acj
tically circular as well as central ; and in this manner a continuous
» S.r llie rcmarUi of Mr D.illlnjcr.-nliMc c.
Iik-l.i-t |im.cr. lo Mm Miuly o( ll.c iiiinutc-1 li.l.
•liULC uLuOJLU^il'8 0bKTVcr.-=-ln Jour. Hey. Ji/ic
in t'lC applirntlon of llie
\\ p! Ol.-.blv ji rulur I li«D
JSor.uDeccmlii;&'iaS2.ji_S5^
MICKOSCOFE
271
Tiew of the object is obtained, witli a m-aJational modification of the
Light. Another motlioJ. coiuuionly adopted in German microseopcs,
is to place a draw-tube in tlto optic axis between tlio stage and the
miiTor, and to diop into tlic top of tliis tube one of a set of " stops "
perforated with apertures of dilfercnt sijics ; this allows a gra-
aational clfcct to bo obtained by i-aisiug or lowering the tube, so as
to place tho stop nearer to or move remote from the object ; but it
is not nearly so convenient as the iiis-diaplu-agin ; and the effect of
the stop is not nearly so good when it is removed to some dis-
tance bencatli the object as when it is very near to the under sui--
face of tlio glass object-slide. Wlicn an achromatic condenser is
used, either a iliapliragm -plate or an iris-diaphiagra should be placed
below its back lens, so as to cut olf any required proportion of tlie
outer mys that fonn its illuminating cone.
Such an arrangement, while suiting all tho ordinary requirements
of tho microscopibt who uses tho higliest powers of his instruuient
for the purposes of biological ijivestigation (as, for example, in tho
study of Bttctci-Ui or of tlie reproduction of the i£unadiiui\ does not
eerve to bring into ctfective uso tlio special resolving power pos-
sessed by objectives of largo apertmc. It has long been known
that for tho discorumcut of very closely apnro-xinjatcd markin;;3
oblique illuminatiou is advantageous, — anobjectivo which exiiibits
such 8 diatoiu-valvo as Plcuyovigiuti augtJattiiii with a smooth un-
marked surface when illuminated by the central rays of tho achro-
Diatijc condenser making its characteristic markings (figs. 8-11)
Sistiuctly visible when the central rays of tho condenser arc kept
back by a stop, aud the object is illuminated by its couvergent mar-
ginal rays only. And it has also been practically known for souie
time that tlio resolution of lined or dotted tests can be often
effected by mirror illumination alone, if the miiTor bo so mounted
as to be able to reflect rays through the object at such oblit|uity to
the optic axis of tlie microscope as to reach tho margiii of a widc-
anglcd objective. Cut it has only been since Professor Abbe's
researches havo givcji tho true theory of "resolution" that tlio
special advantage of oblique illumination has been fully compre-
hended, an<l that the best means liave been deWsed for using it
effectively. Two dilfcrent systems have now come into use, each
of wlUch ha*s its special advantages.
One consists in tlio attadiiuent of tho illuminating appaiatus
(miiTor and achi-oinatic coiidcnscr) to a ** swinging tail-piece " (see
fig. 3'2), whidx, moving radially upon a pivot whoso axis intersects
the ontic axis at right angles in tljo plane of tlio object, can trans-
mit tlie illuminating i)cncil through it at auy degree of oblitjuity
that the constiniction of tho stigo allows. Tlic directiou of this
pencil being of coui-sc limited to one azimuth, it is requisite, in orilcr
to bring out its full resolving eflect, that the object should bo made
to rotate, by making tlie stage tJiat carries it revolve round the
optic axis, so that thu oblique pencil may impinge ujion tlie lines or
other markings of tho object in every directiou successively. It
will then be found tJiat tlio appearances jiresentcd by tiio same
object often var^ considerably, — one set of lines being shown when
tho object lies in one azimuth, ami anotlier when its azimutli has
been ciiangod by rotation tl>rou''li 6u°, 90", or sonio other angle.
Various contrivances havo also been devised for throwing very
oblique illuminating pencils on the object by lueans of [irisms
placed bcneatli tlic sLige.
innmination of at least equal obliquity to that afforded by tho
swinging tail-)iicco may now, lio-vcver, bo obtained by tho use of
condensers spei ially eonstiuctcd to give a divergence of ITO" to tho
rays which they transmit wlien used immersionally, by bringing
their flat tops into api>io.umation to tlie under sido of the glass
slide on which tho object is moniit^d, with tho interiKj.sition
of a film of water or (preferably) of glycerin. By using a eeiitial
stop, marginal rays alone may In; alluwed to ]>ass ; and these will
bo transmitted tliiungli the obje.t ill ivviy azimuth at the same
time. But diaphragms wiili apellnivs limiiing the transmitted rays
to onu part of tlie periplni y may bo so lixed in a tube beneath
tho condenser as to bo ea.sily made to rotate, thus sending its
obliquo peiii ils through the olijec-t in every azimuth in succession.
Aud wliei-u this rotation of the diaphragm brings out two sets of
lines at o certain angular inteival a dia|.liragm with two margin.al
-oi>eiiiiig« at a lorri'sponding angular distance will enable both to
bo seen .it once. Xniinious arrangements of tliis kind have been
Jcvi.sed by those who devoto their s]ieejal attention to tlio rcxo'
lution of dillienlt diatom-tests ; but tiny are of little or no use to
those who use the microseu[io for biological research.
For tho ilhiminntion of the surfaces id' opaque objects which must
be seen by rellcited liglit tlie means emidoyed will vary with tho
focal length of tlio objective emido\eJ. For large bright obiiets
viewed under a low inagnilying ]<o
sullicient ; but if the snifaeV of th
little li-ht, die aid of a bull's-eyo o
♦ employed in order to give it siilhc
always I« rciiuircd by lamplight ; !
tho rolalivo distances of tliu lauip and the object tho nx\n from the
lamp may bo made either to spread themselves over a wide ana or
to couvergc iipoji a email spot. The former is the method suitablo
to large objects viewed under a low maenifying power ; tho latter
to the illumination of email objects whict are to be examined under
objectives of (say) 1 inch or J inch focus. Another method which
may be conveniently had recoui-se to when the microscopo is pro-
vided with a swinging tail-piece is to tmn this on its pivot until
the concave mirror is brought, above tho stagf, so that lays which
it gathei-s either .from natural or artiticial sources may be reflected
downwards upon tlie s&rface of the object.
Tho illumination of an opaque object to be seen with a higher
power than the j or J inch objectives was formerly provided for
by a concave speculum (termed a Liebeikulin after its inventor), with
a perforation in the centre for the passage of the rays to the objec-
tive to which it is fitted,— the cnrvatuie of the speculum being so
adapted to the focus of the objective which carries it that, when
the latter is duly adjusted, tlic lays
rcllected upwards around the object
fi'om tho mirror to the speculum
shall converge strongly on the ob-
ject. The various disadvantages of
this mode of illumination, however,
havo caused it to bo now generally
superseded by other arrangements.
For powers betw-een lA inch and
^'n iiich, and even for a J or i inch
of small angle and good working
distance, nothing is so convenieut
as the parabolic speculum or side-
illuminator (F, fig. 17) invented by
the late Richard Beck. This is
attached to a spring-clip that slides
on the tubes of low-[iower objec-
tives, so that its distance from the
object and the direction of its re-
flected pencil are rea.lily adjusted ; F'o- 17>— Beck's Parabolic Side-
and for use with higher powers it IHummator, with Crouch's
may be either mounted on a sejiar Adapter,
ate anil attached to some part of the stand of the microscope, or
may be hung in the manner shown in fig. 17 from an '* adapter "
A interposed between the objective and the body. By rotating
the collar B and making use of the joints C, C, the lengthening
rod D, and tlie ball and socket F,, any position may be given to the
speculum F that may best suit the objective with which it is used. \
When, however, it is dcsu-ed to illuminate objects to be seen under
objectives of high power and very short working distance, side
illuminatiou of any kind becomes diflicult, though not absolutely,
impo&sible ; * and various modes have been devised for the illumina-
tion of tlic object by means of light sent down upon it, through
tlio objective, from above. This isdono in the vertical illuminator
of ilcssi-3 Beck (fig. 18) — tho original idea of which was first
rtr gooil oiilinary ilaylighr is
object is dull, ixlleeling but
■ larso bi-convex lens must bo
cut biillianeo. This aid will
nd by a iinqn-r adjustment ot
f ic. 18. —Beck's Vertical Illuminator,
given by the Amoiiean Professor H. h. Smith— by a disk of
thin glaU li, I, atraehed to a milled head by which its angulat
Iioaition may be adjusted, and introduced by a slot A, c into thq
interior of an adapter that is interposed between the objective C, it
and tho nose c of the body. The light which entci-s at the lateral
aperture A, c, falling U)ion the obliciuo surface of the disk C, 6, i^
rellected downwards, and is concentrated by tho lenses of th^
objective upon the object beneath. The lateral aperture may b<J
provided with a diaphragm, with openings of dillerent sizes, foe
diminishing the false light to which this method is liable ; or a sci-eej
witli a small ai'crturc may be placed between the lamp and tlirf
1 .S.T n mnh.ul Jtvlsccl by Mr Jiimn Siiiilli, in Jo'r- R")- Mi<rti. Sof,, voL l^
K. S., ISB'i, v- ^'J^-
272
MICROSCOPE
illuminator, at any distance that is found to produce the best effects.
In using this illuminator, the lamp should be placed at a distance
of about 8 inches from the aperture; and, when the proper adjust-
ments have been made, the image of the flame should bo seen upon
the object. The illumination of the entire field, or the direction of
tlio light more or less to either side of it, can easily be managed by
the interposition of a small condensing lens placed at about the dis-
tance of Its own focus from the lamp. The objects viewed by this
mode of illumination with dry-front objectives are best uncovered,
since, if they are covered with thin glass, so large a proportion of
the light sent down upon them is reflected from the cover (especially
when objectives of large ande of aperture are employed) that very
little is seen of the objects beneath, unless their reflective power is
very high. "With immersion objectives, however, covered objects
may be used. Another method of vertical illumination long since
o&vised by Mr Tolles has recently been brought into notice by
Professor W. A. Rogers of Boston (U. S.). It consists in the in'-
ti-oduction of a small rectangular prism at a short distance behind
the front combination of the objective, so that parallel rays enter-
ing its vertical surface pass on between its parallel liorizontal sur-
faces until they meet the inclined surface, by which they are
i-eflected downwards. In passing tlirough the front combination of
the objective, they arc deflected towanls its axis ; but, as their
angle of convergence is less than the angle of divergence of the rays
proceeding from the object, the reflected rays will not meet in tlio
local point of the lens, but will be so distributed as to illuminate
a sufticieiit area. By altering the extent to which the prism is
pushed in, or by lifting or depressing its outer end by means of a
niilled-head screw, the field of illumination can be regulated. The
working of this prism with immersion-objectives is stated by Mr
Tolles to bo peculiarly satisfactory.
Black-Ground Illumination. — There are certain classes of objects
which, though sufficiently transi»arent to be seen with light trans-
mitted through them, are best viewed when illuminated by rays X>i
such obliquity as not to pass directly into tlie objective, — such a
proportion of tliese rays being retained by the object as to render it
self-luminous, when, all direct li^ht being cut otf, tlio general field
is perfectly dark. This method is particularly effective in the case
of such delicate mineral structures as the siliceo^ tests of Pohj-
cijsiina and the *'frustules" of Dialomaccw. And it is one ad-
vantage of tliis kind of illumination tliat it bi-ings out with
considerable etlect the solid forms of objects suited to it, even
when they are viewed monocularly. Two modes of jiroviding this
illumination are in use, each of which has its special advantages.
One consists in placing a central stop either upon or immediately
beneath a condenser of wide aperture, which shall cut ofi'all rays
save those that, after passing through the object {as in fig, 20),
diverge at an angle greater than that of the objective used ; so
that, while tlio ground is darkened, the object is seen brightly
standing out upon it. But if tlie divergence of the rays is but
moderate (say 60°), and the angle of tlie ob}ect:ive is large (say
90°), the most divergent rays of the condenser will enter the mar-
giual portion of the objective, and, tho. field not being darkened,
the black-ground eff'ect will not be produced. This method
^as the gleat convenience of allowing black-ground illumination
to be substituted for the ordinary illumination under dilfcrent
powers, without any other change in the a]'i^aratus than the turning
of a diaphragm-plate fitted with stojis of dillcrcnt sizes «uitablo to
the several ai>crtures of the objectives ; and the modern achro-
matic condensers of wide a]>erture can he thus used with objectives
of 120° QUfjlc.
An excellent black -gi'ound illumination is also given by tho para-
bolic illuminator (fig. 19), originally worked out as a silvered
sneculum by Mr "Wenham, but now made as a paraboloid of glass
that reflects to its focus the rays which fall upon its internal surlace.
A diagrammatic section of this instrnment, showing the course of
the rays through it, is given in fig. 20, tlie shaded portion repre-
senting the paraboloid. The parallel rays r, ;•', i-", entering its lower
surface i>erpendiculaily, pass on until tlicy meet its jiavabolic
surface, on which they fall at such an angle as to be totally reflcctrd
by it, and are all directed to^^ards its focus F. Tlic top of tlio
paraboloid being ground out into a spherical curve of whidi F is
the centre, the rays in emerging from it undergo no refraction, since
each falls jierpendicularly upon the part of tlio surface through
which it passes. A stoj) placed at S prevents any ^t' the ravs
reflected upwards by the mirror from passing to the object, whic)i,
being placed at F, is illuminated by the rays reflected into it from
all sides of the paraboloid. Those lays which i>ass tlirough it
diverge again at various angles ; and if the least of these, GFIi, be
greater flian the angle of aperture of the object-glass, none of them
can enter it. The stop is attached to a stem of wire, which pasM's
vertically tlirough the paraboloid and terminates in a knob beneath,
as shown in fig. 19 ; and by means of tliis it may be inislicd
upwards, so as to cut olf the less divergent rays in their pasi^a^.'c
towards the object, thus giving a black-ground illumination with
objectives of an angle of aperture much wider than GFH. In lising
the paraboloid for delicate objects, the rays \\hicli are made to enter
it should be parallel ; consequently tho plane mirror should alwajs
be omi)loycd ; and when, instead of the parallel rays of daylight, we
are obliged to use th
rendered as parallel a;
the mirror, by tho
interposition of tho
" biill's-eyo " so ad-
justed as to produce
this eflVct. There are
many cases, however,
lamp, thoso should be
possible, previously to their reflexion from
i*arabohc llJuuiinulur.
in which the stronger light of tho concave mirror is i»referable.'
When it is desired that the light should fall on the object from one
side only, the circular oi^^ning at the bottom of the wide tube that
carries the paraboloid may be fitted with a diaphragm adapted to
cover all but a certain portion of it ; and, by giving rotation to
this diaphragm, rays of great obliquity ma/ bo made to fall upon
the object from every azimuth in succession.
In order to adapt this paraboloid to objectives of very vdde angle
of aperture, a special modification of it, originally devised by Mr
"Wenliam, has been latterly reintrodu'^*.! under the designation ol
"immersion-paraboloid," with most .xocllent cH'cct. This consists
in making the top of the paraboloid flat instead of concave, antl in
interposing a film of glycerin between its surface and tho under
surface of the glass slide carrying the object. Only rays of such
extreme obliquity are allowed to pass into the slide as would bo
totally reflected from its under surface if they fell upon it through
air ; and, as these illuminate tlio object without passing into tlie
objective, it can be thus examined under even the liigliest powera.
/BiKOCULAn MiCKOSCOPES. •
Stereoscopic Binoculars. — The admirable invention of the stereo-
scope by Professor AVhcatstonc has led to a general apjirecia-'
tion of the value of tlie conjoint use of both eyes, in convoying to
tho mind a concei)tion of the solid forms of objects such as the
uso of either eye singly docs not generate with tho like certainty or
eflcctivencss (see SxtuEoscorK). This ronccjition is tho product
of tho mental combination of the dissimilar ppi-spirtivc projections
which our right and left rctiiuv receive of any object that is suffi-
ciently near the eyes for the formation of two im.igcs that are sen-
sibly dissimilar. Kow it is obvious that a similar diflcrenrc must
exist between the two perspective jnojections of any object in relief
that are formed by the right and left halves of a microscoiiic ob-
jective and that this difl'crenoc must increase with the angular
aperture of tho objective- And tho fact of tliis diflcrcncc ni.-iy be
easily made ap}tarent cxj>erinicntally, by adaptin^^ a semicircular
"stop" to any objective of from 20"' to 30" auglo in such a manner
that it can be turned so as to cover cithx-r its right or its left half;
for not only will the two images of any projecting object formed by
the rays transmitted through the two uncovered halves be found
sensibly difl'cicnt, but, if they be ]'hotographed or accurately drawn.
tho "pairing" of their pictures in the stereoscope will bring out
tho form of the object in vivid i\-licf. What is needed, thereforc^to
give tlic true stereosropic cOcvt to a binocular niicioefopo is a means
of so bibi-ctinj: the cone of rays transmitti-d by tho objective that
iti two hiteralhalvcs shall be transmitted the one to tho right ami
the other to the left eye, and that tlic two images shall be crossed
(tho image formed by the right half of the ohirctivc being sent lo the
left eye, and that fbrmcd by tlie left lialf of tlic ob>ctivi' Ik iiifi sent
to the right ere) in ordi-r to neutrali;;o tho rcvci-siii;; cHcct of the
niicroscoj.c itself. If this crossing docs not take place, the 'effect
will bo rendered "pscudosropic." not "orthos.opic," — its projec-
tions becoming depressions, and itsde]Uvssioiis being brought out as
prominences. It was from a want of due ajqireciation of this fact
that tlio earlier attempts at constructing a stereoscopic binocular
gave representations ot objcvis }tlaeed under it, not in their true
orthoscopic, but in their pseudoscopic as]>ect. Tliis . was^ tho
case, lor c:wmplcj witlL-tU&'oinocuhu'-microscoDC first..dcvi:»odU>^
MICROSCOPE
273
Professor Hidden of Kew Orleans in I8SI, which separated the cone
•f rays by a pair of rectangular pxisms so placed edge to edge above
the objective that the rays pacing through its right half were
refiected horizontally to the right side, to be changed to the vertical
direction and sent to the right eye by a lateral rectangular pi-ism,
while the rays from the left half of tlie objective were sent to the
left eye in a similar manner. Professor Rlddell describes the
"conversion of relief" produced by this arrangement with the
ordinary eye-piece as making a metail spherule appear "as a glass
boll silvered on the under side, and
a crystal of galena like an empty
box. And to render the images
4* normal and natural " he found
himself obliged to use erecting eye-
pieces, which should produce a second
reversal of the images that had been
reversed in their first formation.^
Subsequently, however. Professor
Biddell devised and perfected another
arrangement giving a true orthoscopic
effect, which, after being long disre-
garded, has been latterly taken up
and brought into use by Mr Stephen-
eon. The cone of rays passing up-
wards from the objective meets a
pair of prisms (A, A fig. 21) fiied
immediately above ita back lens,
which divides it into two halves ;
each of these is subjected to internal
reflexion from the inner side of the
prism through which it passes; and _ „, r,,, ,, t>- ,
the sUght separation of the two prisms ^'°- ^'"^S ' B""''^'"
at their upper end gives to the two
pencils B, B, on their emergence from the npper surfaces of the
prisms, a divergence which directs them through two obliquely-
placed bodies to their respective eyepieces. By this internal
reflexion a lateral reversal is produced, which neutralizes that of
the ordinary microscopic image, so that, while eaclx eye receives
the image formed by its own half of the objective, the pairing
of the two pictures produces a true orthoscopic effect'
About the same date MM. Nachet of Paris succeeded in devising a
binocular that should give a true orthoscopic image, by placing above
the object-glass an equiangular prism fP. fig. 22) with one of Its sur-
faces paraUel to its bacK leus, ,
which, receiving the pencils ab
forming the right half of the
cone, iutemally reflects them
obliquelv upwards to the left,
and in like manner reflects the
jiencils a'b' from the left half of
the cone obliquely upwards to
the right. These pencils, pass-
ing out of the left and right
oblique facea of the prism at
right angles (so as not to undergo
either refraction or dispersion),
enter right and left lateral
prisma, also at right angles, and,
after being internally reflected
hy these, pass out verricilly, ui
right angles to their upper sur
fares, through two parallel bot.lies
(fig. 23), wiiose eve-pieces bring
them to a focus" in the right Flo. 2i— Nachct's BinocuJar
and left eyes respectively. The Prisma.
distance between these bodies may be adjusted to the varying
distances between the axes of individual paira of eyes, by adjust-
ing screws at tlieir base, which vary the distance of the lateial
prisms from the cential. Tliis instrument gives a theoretically
Iterfcct representation of a microscopic object in relief, as it would
appear if enlarged to the size of its image, and brou"ht to within
about 10 inches of the eye ; and its chief practical defect is that,
as the two bodies are parallel, instead of being slightly converg-
ent, it cannot be continuously used without an uncomfortable
strain. But as its performance depends upon the accuracy of the
seven plane surfaces of the three prisms, and on the correctness of
their relations to each other, it is liable to considerable error from
inil>erfections in its construction ; and, as the instrument can only
be used for its owu special purpose, the observer must bo provided
with an ordinary' single-bodied microscope for the examination of
objects unsuited to the [owere of the binocular. This last objection
^•pplies also to Professor Riddell's model.
, It was for these reasons that Mr Wcnham, fully impressed with
ihe advantages of steiieoscopic vision to the microscopist, set himself
(•'lo. 23. — Nachet's Binocular
Microscope.
• Sm EitUman's /ourmrf, rol. iv., 1*53, p. CS ; and Quart. Jour, cf Ulcroi.
Bci.. vol. L, 1863, p. J36.
» Quvl. Jtur. tf Hunt. Set., rcl U., 13M. p. li
to devise-a construction by which it might be obtained without tlo
drawbacks inevitable in the workingof Kiddell's and Uachetfi instru-
ments; and he soon succeeded in accomplishing this on apian which
has proved not only convenient but practically satisfactory, notwith-
standing its theoretical im-
perfection. Only the right
naif of the cone of rays pro-
ceeding upwards from the
right hau of the objective
(a, fig. 24) is intercepted by
a pnsra placed immediately
over that naif of its back lens,
which, by two internal re-
flexions (as shown in fig. 25),
sends its pencils obliquely
upwards into the left-hand or
secondary body L, whilst the
pencils of the left half-cone
pass uninterruptedly into the
right-hand body R, and form
an image that suffers no other
deterioration than that which
results from the halving of the
angular apertuie and the con-
sequent loss of light The
moderate convergence of the
two bodies (which, by vaiying
the angles of the prism, may
be made gi-eater or less, so as
to accord with the ordinaiy
convergence of the optic axes "
in the individual observer) is '
much more generally suitable
than the parallelism of MM.
Nachet's earlier instrument;
and the adjustment requisite for variation of ^Ustauce between the
eyes can be made by simply lengthening or shortening the bodies
by drawing out or pushing in tbe diverging h
eve-pieces.
It may be fairly objected to Mr Wenham's
method (1) that, as the rays which pass ,
through tbe prism aud are obliquely reflected
into the secondary body traverse a longer
distance tlian those which pass on uninter-
ruptedly into the principal body, the image
formed by them will be somewhat larger than
that which is formed by the other set, aud (2)
that the image formed by the rays which have
been subjected to the action of the prism must
be inferior in distinctness to that formed by
the uninterrupted half of the cone of rays.
But these objections are foimd to have no
practical weight For it is well known to
those who have experimented upon the phe-
nomena of stereoscopic vision (1) that a slight
difference in the size of the two pictures is no
bar to their perfect combination, and (2) that,
if one of the pictures be good, the full effect
of relief is given to the image, even though
the other picture be faint and imperfect, pro-
vided tliat the outlines of the latter are suffi.'
ciently distinct to represent its perspective
projection. Hence if, instead of the tivo
equally half-good pictures which are obtain-
able by JIM. Nachet's original constiuction,
we had in Jlr Wenliam's one good and one Fio. 24.— Wenhaiu"s
indifferent |.icture, the latter would be de- Stereoscopic Ein-
cidedly preferable. But, in point of fact, the ««="'»'■ Microscope,
deterioration of the second picture in Mr Wcnham's aiTangement
is less considerable than that of both pictui-es in the original
arrangement of JIM. Nachet ; so that the optical performance of
the Wenliam binocular is in every way superior. It has, in addi-
tion, these further advantages over the preceding : — first, the
greater comfort iu using it (especially for some length of time
together) which resultji from the convergence of the axes of the
eyes at their usual angle for moderately near objects ; second, that
this binocular arranc;enient does not necessitate a special instrument;
but may be applied to any microscope which is capable of carry-
ing the weight of the secondary body,— the prism being so fixed
iu a movable frame that it may in a moment be taken out of
the tiilM or replaced therein, so that when it has been removed the
principal body acts in every respect as an ordinary microscope,
the entire cone of rays passing uninterruptedly into it ; and, thiitj,
that the simplicity of its constniction renders its derangement
almost impossible. Hence it is the one most generally preferred
by microscopists who use the long-bodied English model.
* for short-bodied Coutinental microscopes, however, MM. Nachet
274
MICROSCOPE
;'.avo iloviaed an arranTCmom of two prisms, baseil on Mr Wcnliam's
' iiiilanic:ital iilca of ilcllccting one lialf of tlio cono of rays into a
icconilary boily, whilst the other half proceeds onwards withont
change of direction into the principal body. Ami it is an interest-
ing fe.iture in tliis construction that, by a siinnle change in the
liosilion of the dividing prism, thc'true "orthoscopic" image may be
inadc, by a " convoi-sion of relief," to become " pseuiloscopic." *
- - - ' ' ■ ■ d, howev
The clfect of stc
/imMis.
Flo. 25.— Weill.;
cuiar
projection may bo attained, however,
Trithout a double body, b"y tlio insertion of a suitably constructed
Linocular c^-c-picco into the body
of any ordinary monocular micro-
Bcope. A plan of this hind was
first successfully Ivorhcd out by
JIrTollc3 (the very ablo optician
of Boston, United States), who
ijitc-rposcd a system of prisma
similar to tliat devised by ilM
Kadiut (fi^,'. 22), but on a much
larger scale, between an "erector"
(roscnibliiiK that used in tho eyo-
piceo of a day telescope) and a i>air
of ordinary Huygenian cyc-piccea,
tlio central or dividing prism
being placed at or near tlie jdano
of the secondary inia"o formed by
the erector, while tlio two eye-
pieces are jdaced immediately ^..^^
above tlio lateral prisms, — the ».-"•-
combination thus making that division in the pencils forming the
secondary (erected) image which it makes in the Nachet binocular
in the pencils emerging, from tho objective.
A stereoscopic eye-piece of a very difTereut construction has been
recently devised by Professor Abbe, who, making use, for the
Jivision betWL-en the two eye-pieces of tho rays going to form the
first imago, of an arrangement of prisms essentially similar to that
devised by 5Ir Wenham for his non-stereoscopic binocular (fig. 27),
obtains eitlur an orthoscopic or a pseudoscopic etTect by placing
oil each cyu-piece a rap with a semicircular diaphragm, so as to
extinguish half of each of the cones of rays that form tho two
n-tinal images. AVhilo in one position of the diaphragms truo
stereoscopic or orthoscopic relief is given, it is sufficient to turn
the diaphragms into the opposite position to obtain a pseudo-
'scopic convL'i-sion.^ It apjiears, however, that this arrangement,
though possessing points of gi-eat interest in relation to the theory
of binocular vision, is not likely to supei-scde the ordinary Wenham
prism.
It must be obvious to every one who studies with sufficient
ntteutiou tho conditions under which true stereoscopic relief can be
given that no combination of two dissimilar retinal perspectives
can bo satisfactory unless the visual pictures represent with tolerable
distinctness the features of the object that lie in dilferent focal planes.
This is provided for, in ordinary vision, by the power of accommo-
dation possessed by the eye, which, while focussed exactly to any
one jilanc, can also inrludo in its visual picture (within certain
limits) what is either nearer or more remote. Now it seems prob-
able that, as Professor Abbe has urged, this power of accommoda-
tion comes into play in microscopic stereoscopy, but there can be
no question that the visual distinctness of the parts of an object
lying within and beyond the focal plane, and tlierefore the com-
Sletencss of tho stereoscopic image, mainly depends upon the "focal
epth " of tho objective employed,— which, as alrcaify explained, is
a function of its angular aperture. \Vlien, however, objectives of long
focus and small aperture are employed in binocular microscopy,
although each of the two perspective projections may be fairly
distinct throughout, tho efToct of solid relief will be very incon-
siderable, because the pictures are not gufficiontly dissimilar to one
anotlier, — the case being exactly analogous to titat of tho stereo-
scopic combination of two photographic portraits taken at an angle
of no more than a few degrees from each other. Still, with an
objective of 1^ inches focus and an angular aperture of from 15° to
20", a very distinct separation is made of tlic focal planes of trans-
parent sections of structures having no great minuteness of detail,
— such, especially, as injected prepai-ations, — tho solid forms of
their capillary networks being presented to tho mind's eye witli a
.vividness that no monocular representation of them can afford.
["VNMien a 1 inch objective of 20° or 25° is used, the stereoscopic effect
becomes much more satisfactory ; so that objects of moderate pro-
jection (s\ich as many of tho siliceous Pohjci/stina, Diatomaccre^
i;c. )can bo seen in nearly their natural projection, and, if the focal
adjustment is made for a medium plane, with tolerable distinctness
iboth of their nearer and remoter parts. With a 3 i'i<^h of 30° or
'35°, the stereoscopic relief becomes more pronounced ; but the
idiminution of the focal depth prevents tho several planes of objects
ixn strong relief from being as distinctly seen at tho same time. A
\ inch objective of abotit 40* of aportnre, however, affords the most
satisfactory results with suitable objects, — full stereoscopic relie/
being gained \\'ithout exaggeration, so as to present, e.g., the
discoidal diatoms and the smaller Polycystina in their true forms,
whilst their nearer and more remote parts are seen with sufficient
distinctness to require only a very slight adjustment of the focua
for their perfect definition. Still more minute objects may be welt
shown by j^ths and jth objectives whose angular aperture does
not exceed 50° ; but it can be shown both theoretically and
practically ' tliat the dissimilarity of the two perspective projections
of objects in relief formed by objectives of any angle much exceed-
ing 40' is such as to exaggerate the stereoscopic effect ; besides
wliich, every enlargement of angular aperture so gi-catly diminishes
the focal depth of tho objectires that only those parts of the objects
which lie very near the focal piano can bo seen with distinctness
sufficient for the formation of a good stereoscopic image. Henco,
for the purposes of minute histological research, the stereoscopic
binocular is (in the present writer's opinion) almost valueless ;
since, if any distinct perspective differentiation can be gained with
objectives of the short focus and enlarged angle that are n\Q^,
suitable to such investigations, that differeutiatiou will be so great
as to produce a highly exaggerated stereoscopic effect If such
objectives be used binocularly at all, they must be so mounted that
their back lenses are in very close proximity to the prism ; and the
(transparent) object must be illuminated by an achromatic condenser
of sufficient aperture to send through it pencib of sufficient diver-
gence to produce the secondary image.
In regard to the advantage derived from the use of the stereo-
scopic binocular, witli tho powers, and upon tho objects, suitable to
produce the true etfect of solid form, tho writer can unhesitat-
ingly assert, as the result of a long and varied experience, that
in no other way could he as certainly or as vividly image those
forms to himself, and that in prolonged work upon such subjects
he is conscious of a great saving of fatigue, which seems attributable
not merely (perhaps not so much) to the conjoint use of both eyea
as to tho absence of the mental effort required for the interpretation
of the microscopic picture, when the solid form of the object has to
bo ideally consti-uctcd from it (chiefly by means of the information
obtainable through the focal adjustment), instead of being directly
presented to the mind's eye.*
Non-Sicrcosco^nc Binoculars. — The great comfort which is experi-
enced by tho microscopist in the conjoint use of both eyes has led
to the invention of more than one avrangement by which this can
bo secured when those high powers aro required which cannot be
employed with the ordinary stereoscopic binocular.
This is accomplished by Messrs Powell and Lea-
laud by taking advantage of the fact that, when a
pencil of rays falls obliquely upon the surface o|
a refracting medium, a part of it is reflected with-
out entering that medium at all. In the place
usually occupied by the Wenham prism they
interpose an inclined plate of glass with parallel
sides, through which one portion of the rays pro-
ceeding upwards from the whole aperture of the
objective passes into the principal body with very
little change in its course, whilst another portion
is reflected from its surface into a rectangular
prism so placed as to direct it obliquely upwards
into tho secondary body (fig. 26). Although
there is a decided difference in brightness between
tho two images, that formed by the reflected rays
being the fainter, yet there is niar\'ellously little
loss of definition in either, even when the ,', inch
objective is used. Tho disk and prism aro fixed * '° ""'
in a short tube, which can be readily substituted in any ordinary
binocular microscope for the one containing tho Wenham prism.
Other arrangements were devised long ago by Mr Wenham,' with
a view to obtain a greater equality in the amount of light-rays form-
ing the iwo pictures ; and he has latterly
carried one of these into practical effect,
with the advantage that tho compound
prism of which it consists has so nearly
the same shape and size as his ordinary
stereoscopic prism as to be capable of
being mounted in precisely the same
manner, so that tho one may bo readily
excliangcd for tho other. The axial ray a,
proceeding upwards from the objective,
enters tho prism ABDEF (fig. 27) at p. 07
right angles to its lower face, and passes
on to c, where it meets tho inclined face AB, at which this prism'
is nearly in contact with the oblique face of the right-angled
» See Tram, of Iloy. Micros. Soc, N. S., vol. xt., 18C7. p. 105 ; and Monthly
[Bln-oi. Jour., vol. I., 1300, p. CI.
* SCO Jour. (t/Rov- Micro*. Soc., 2d sot., vol. !.. 1881, p. 208.
» See The Miei-oseope and its Rrrefationi, Cth cd.. pp. 42-^4. -
♦ Avery clabomte InvpsllRntlon, by Prolcssor Abbe, "On the Conditions m
Oilhoscopic onil I'scudosrorlc Effects In tho Binocular Mlcroscop«," *U1 bo (oual
In tlio Jour, of tfie Roy. Micros. Soc., 2d iter., vol. I.. ISSI. p. 203.
ft Traruaetioru nftht Micpvs, Soe., N. S., vol. xiv., I860, p. 103.
MICROSCOPE
275
Tcism ABC. By internal reflexion from the former and ext€mal
reflexion from the latter about half the beam b is reflected within
the- first prism in the direction cb, while the other half proceeds
straight onwards through the second pnsra, in the direction ca\
«o as to pass into thtf principal body. The reflected half, meeting
■t d the oblique (silvered) surface DE of the first prism, is again
reflected in the direction db'^ and, passing out of that prism per-
pendicularly to it3 surface AF, proceeds towards the secondary
body. The two prisms must not be in absolute contact along the
plane AB, since, if they were, Newton's rings would be formed ;
and much nicety is required in their adjustment, so that the tuo
reflexions may be combined without any blurring of the image in
the secondary body.
For the prolonged observation, under high powers, of objects not
requiring the extreme of perfection in definition, — such, for example,
as the study of the cyclosis in plants, — great advantage is gained
from tlie conjoint use of both eyes by one of the above arrangements.
Mechanical Construction of the Microscoi-e.
The optical arrangements on which the working of the compound
achromatic microscope depends having now been explained, we have
next to consider the mechanical provisions whereby they are brought
to bear upon the different purposes which the iustrumeut is destined
to serve. Every complete microscope must possess, in addition to tlie
lens or combination of lenses which affords its magnifying power, a
stage whereon the object may securely rest, a concave mirror for the
illumination of ti'ansparent objects from beneath, and a coudeusing-
lena for the illumination of opaque objects from above.
1. Now, iu whatever mode these may be connected with each
other, it is essential that the optical part and the stage should be
80 disposed as either to be altogether free from tendency to vibra-
tion or to vibrate together ; since it is obvious that auy movement
of one, in which the otlier does not partake, ^vill be augmented to
the eye of the observer in proportion to tho magnifying power
employed. In a badly-constructed instrument, even though placed
upon a steady table resting upon the firm floor of a well-built house,
wneu hi^'h powers are used, the obiect is seen to oscillate so rapidly
at tlie slightest tremor — such as that caused by a person walking
across the room, or by a carriage rolling by in the street — as to be
frequently almost indistinguishable ; whereas in a well -constructed
instrument scarcely any iieiccptible effect will be produced by even
greater disturbances. Hence, in' the choice of a microscope, it
should always be subjected to this test, and should be unhesitatingly
rejected if the result be unfavourable. If the instrument should be
found free from fault when thus tested with high powers, its
stcadines with low powers may be assumed ; but, on the other
hand, though a microscope may give an ima^e free from perceptible
tremor when the lower powera only are emmoyed, it may be ijuite
unfit for use with the higher. The method still adopted by some
makers, of aupiiorting the body by its base alone, is tho worst
possible, especially for the long body of the large English model,
since any vibration of its lower part is exa^^gerated at its ocular end.
The firmer the support of the body along its length the less tremor
will be seen in the microscopic image,
2. The next requisite is a cai>ability of accurate adjustment to
every*variety of focal distance, without movement of the object. It
is a principle universally recognized in the construction of good
microscopes that the sta^e whereon tlie object is placed sliould be
a fixture, the movement by which the focus is to be adjusted being
given to the optical portion. This movement should be such as to
allow free range from a minute fraction of an inch to three or four
inches, with eaual power of obtaining a delicate adjustment at any
part. It should also be so accurate that the optic axis of the iu-
sti'ument should not be in the least altered by any movement in a
Tcrtical direction, so that, if an object be brought into the centre of
the flcld with a low power, and a higher power be then substituted,
the object should be found in the centre of it*, field, notwitlistand-
ing the great alteiution in the focus. In this way much time may
often be saved by employing a low power as a "finder" for an object to
be examined by a higher one ; and when an object is being viewed
by a succession of powers little or no readjustment of its place on
the sta^ should be required. A rack-and-piuion adjustment, if it
be made to work both tightly and smoothly, answera sufficiently
well for the focal adjustment, when objectives of low power only are
en»ployed. But for any lenses whose focus is less than half au inch
a " fine adjustment," or "slow motion," by means of ascrew-move-
Snent ojierating either on the object-glass alone or on the entire body
(preferably on the latter), is of great value ; and for the highest
)K)wer8 it is ouite indispensable. It is essential that in this motion
Ihere should be no "lost time," and that its working should not
produce any " twist " or displacement of the image. In some niicro-
eco^ which are provided with a fine adjustment tlie rack-and-
pinion movement is dispensed with, the "coarse adjustment " being
given by merely sliding the body up and down in the socket which
grasps It ; but this plan is only admissible where, for the sake of
extreme cheapness or portability, the instrument has to be reduced
to *^c form of utmost simpUcity, as iu Hgs. 28. 29.
3. Scarcely lees important than the preceding requisite, in thfl
case of the compound microscope, especially with the long body of
the ordinary English model, is the capability of being placed in either
a vertical or a horizontal position, or at an* angle with the horizon,
without deranging the adjuBtment of its parts to each oth^r, and
without placing the eye-piece "in such a position as to be incon-
venient to the observer. It is certainly a matter of surprise that
some microscopists, especially on the Continent, should still foreg;
the advantages of the inclined position, these being attainable by a
very small addition to the cost of the instrument ; but the incon-
venience of the vertical arrangement is much less when the body
of tlie microscope is short, as in the ordinary Continental model ;
and there are many cases in which it is absolutely necessary that
the stage should be hoiizontal. This position, however, can at any
time be given to the stage of the inclining microscope, by bringing
the optic axis of the instrument into the vertical direction. In
ordinary cases, an inclination of the body at an angle of about 55*
to the "horizon will usually be found most convenient for uncon-
strained obser\'ation ; and the instrument should be so constructed
as, when thus inclined, to give to the stage such an elevation above
the table that, when the hands are employed at it, the arms may
rest conveniently upon the table. In this manner a degree of
support is attained which gives such free play to the muscles of the
hands that movements of the greatest nicety may be executed by
them, and the fatigue of long-continued observation is gi-eatly
diminished. When the ordinary camera lucida* is used for diawing
or measuring, it is requisite that the microscope should be placed
horizontally. It ought, therefore, to be made capable of every such
variety of position ; and the stage must of course be provided with
some means of holding the object, whenever it is itself placed in
such a position that the object would slip down unless sustained
4. The last principle on which we shall here dwell, as essential
to the value of a microscope designed for ordinary work, is simpli-
city in the construction and adjustment of every part. Many in-
genious mechanical devices have been invented and executed for
the purpose of overcoming difficulties which are in themselves really
trivial. A moderate amount of dexterity in the use of the hands ia
sufficient to render most of these superfluous ; and without such
dexterity no one, even with the most complete mechanical facilities,
will ever become a good microscopist. There is, of course, a limit
to this simplification ; and no arrangement can be objected to on
this score wnicli gives advantages in the examination of difficult
objects, or in the detenninatiou of doubtful questions, such as no
simpler means can afford. The meaning of this distinction will
become apparent if it be applied to the cases of the mechanical
stage and tlie achromatic condenser. For, although the mechanical
stage may be considered a valuable aid in observation, as facilitating
the finding of a minute object, or tlie examination of the entire
surface of a large one, yet it adds nothing to the clearness of our
view of either ; and its place may in great degree be supplied by the
fingers of a good manipulator. On the other hand, the use of the
achromatic condenser not only contributes very materially, but is
absolutely indispensable, to the formation of a perfect image, in the
case of many objects of a difficult class ; the want of it cannot be
compensated by the most dexterous use of the ordinary appliances ;
and consequently, althouc^h it may fairly be considered supei-fluous
as regards a lar^^e proportion of the purposes to which the micro-
scope is directed, whether for investigation or for display, yet as
regards the paiticular objects just alluded to it is a no less necessary
part of the instrument than the achromatic objective itself.
As a tj'pical example of the simplest form of compound micro-
scope that is suitable for scientific research, — which, with various
modifications of detail, is the one generally employed on the Con-
tinent,— the Microscope de dissection ci d'obsei~vation (fig. 28) of 11.
Nachet, es|)ecially as constructed for portability (figs. 29-31), seems
particularly worthy of description. In its vertical fonn (fig. 28) the
solid foot to which the mirror is pivoted gives support to the
pillar F, to the top of which the stage P, having a dianhragm-plato
neneath it, is firnily attached. On the top of tliis pillar the tubu-
lar stem A is fitted in such a manner that it may be removed by
unscrewing the large milled head L, — though, when this is well
screwed down, the stem stands quite firnily. This stem beai"s at
its summit a short horizontal arm, which carries a strong vertical
tube that firaily grasps the "body" of the microscope, while per-
mitting this to be easily slid upwards or downwards, so as to make
a "coarse adjustment" of ^he focus. The " fine adjustment" is
made by turning the milled head V, which either presses down tho
outei tube of the stem, or allows it to be raised by the upward pres-
sure of a strong Apiral spring in its interior. By unscrewing iho
milled head L, the stem A with its arm and compound body can be
detached from the pillar ; and, a small li^ht arm H holding cither
aiiigle lenses or doublets being slid into this, a convenient dissecting
microscope is thus proHded. The only drawback in the construc-
tion of this simple model is its not being provided with a joint for
276
MICROSCOPE
tlie inclinaHon of fho bmly ; but this is introdncetl into the port
able form of the iustninient shown in fig. 29, tlic basal i>ortion of
which (fi^. SO) can be uscil, like thnt of the preceding nioilcl, as a
eimple microscope, and, by a most ingenions construction, can be
80 folded as to ho flat in a shallow case (fig. 31) that holds also tho
upper part with tlie objectives of both the simple arm and the com-
Fio. 23. — Nacbet's Combined Sbnple and Compound Microscope.
£onnd body. M. IKachet now connects his objectives uilh tho
odv of his microscopes, not by a screw, but by a cylindncal fitting
held in place by the pressure of a siuing-dip against a projecting
^houldcr. This mcthotl not only allows one objoctivo to be re-
moved and replaced by another much more readily than does the
acrcw-fittiug, but also rcudei-s the centring of diliercnt objectives
more exactly cou-
ibnnable. It may
be safclv aftinncd
that a very largo
proportion of tlio
uiicroscojiic work
of tlie lasr half-
continy, which has
given an eiftircly
new aspect to bio-
logical science, has
been done by in-
stmmcnts of this
siiiiplcCoutiuental
ty,H.
A larger model,'
liowever, was from
the fii-st adopted
by English opti-
cians; and, as a
t\-picnl example of
the general jdan
of construction
now most followed
both in England
and in the United
Stat.'s, the imr
provcvi Jackson-
Zontmavcj- micro- _ „^ »- , » „
scoiw of Messrs '^'^- ""•— ^f»chet s Portable Compound Slicroscope.
Kos^(tig. 3'2) may be appropriately selected. The trii«id baM' of
thi-* instrument carries two pillars, bctwirn which is swung uiKin a
hnrizontal axis icapable of being fixed in any i>osition by a tighten-
ing screw) a solid "limb," wit^i wliirh all tlie other parts of the
inHtrnnient aiv connected, — aplanof cousrniction originally deviled
by Mr Ocorgo Jackson. The binocular body, haviu" at its lower end
ta-( in tig. 24) an onening into which citlic'r of tlie \\Vnhnm yrmm
can be inserted, and at its top a rack movtinent for ailjustuig the eye-
pieces to the distance between the erea of the observer, is attached
to a racked slide, which is so acted on bv the large doublo nulled
Fio, 30, — Nacliet's Portable Dissecting Microscope; on the left as set
up for use, on the right as having the stage P turned back ujjou the
joint O, so as to lie Hut on the bottom of the case.
head^ ift tho njipcr part of the limb as to give a " quick '* upward or
downward motion to tlio bodv; while the "slow" motion, or fine
Fig. 31. — Xacbet's Portable Conipound and Dissecting Mirrosccp .
as packvtl in ca.ic
adjustment, is given by means of the vertical micrometer ^^tcw at
tho back of the Hmb. wliich raises or lowei-s a second «Udc bcUud lU*.
rack.* Tlie stage is
supported ui>on a
firm ring, which is
immovably fixed,
not to the lind>. but
to a strong conical
]nvot which p^-^^.
through the limb, to
be clampvd by a
screw-nut at ir>*
bnck, — the jmrprt^Lo
ofthisbeingtoallow
the whole stage to Ihj
inclined to one side
or the other at any
angle, so that a solid
object maybe newod
Rideways or Ironi
bi.'low, as well as
I'lom above. l'i>oii
this ring the stage
rotates horizontally,
its anc;nlar move-
meuf I'cing mca-
^urcdbvagl■aduatc.l
scale and vernier at
ita edge : aii.l il can
W fixed in anyazi
ninth by nelaininng-
sci-ewhcncath. Kect-
angular movement /jj
is given to the
traversing plarform
which carries The ob- Kic. 32.- Ko
ioct by two milled PI.cro^.oiH,-.
heads on the right of tin- stage, th<^ whole construetinn of wlticli u
adapted to allow light ol extreme o'iiJi.|niry to W ihi^wn niKni ihe
object from beneath. On tin.- strong pivot by which the Mage is.
' mnkcr« tlie fino
vcr ( onnonrd
t In tho oilier form of rnnslnirllMi frill jYtnloiil
n4)4srmciit aci« Uiivi.il> on llie objvcilte. itu- it rii- i
u)! mill duwn witiiin ilu- ^o^c of I'uc hody ; bin thU |>i.
(.-UJ.J \<ltli luaiijr
MI'CROSCOPE
277
attached to the limb (the axis of which passes through the point at
xthkh the object-plane is intersected oy the optic axis of the
body) is hung the swinging tail-piecd invented by Mr Zentmayer of
Philadelpliia, which, carrying the whole illuminating apparatus,
may be so set as to ^ive to the axis of the illuminating pencil any
required degree of ooliquity. To the upper part of it is attached
a rack-and-pinion moTeinent carrying the "substage," which is
provided with two railled-headed screws for centiing it pre-
cisely with the raicrosco]>e-body. Into this may bo fitted the j
achromatic condenser, parabolic illuminator, polarizing prism, or }
any other kind of illuminating apparatus ; whilst at its lower end i
it carries the mirror, the position of which may be varied by sliding !
its fitting up or down the ** tail-piece," or by turning the arm {
which canies it to one side or the other ; while, if direct illumina-
tion from a lamp should be preferred, it may be turned altogether
aside. By swinging the tail piece round above the stage, oolique
light may be reflected from the mirror, through the condenser, upon '
the upper surfaces of objects. The condenser usually fitted to j
this instrument is ">f about iV i»cli focus, with a largo back lens ; |
behind whicli are placed an iris-diaphragm for reducing the light
to the central rays, and a diaphragm-plate with apertures of the
various forms moet suited for the resolution of lined objects by
oHiquo rays.
No instrumcut, in tha writer's judgment, is better adapted than
this for the highest purposes of microscopical research. It works
admirably with ovoTy power from the lowest to the highest, and is
capable of receiving any one of the numerous pieces of apparatus
which liave been devised for special researches of various kinds.
The iletailcd description of these not being here admissible, it will
bo sulficieut to indicate the polariscope and the spectroscope as the
most important of these accessoiies.
MicROinrmv^
The micruscopist has constant need of some means of taking exact
nicesvii-ements of the dimensions of the minute objects, or parts of
objects, on the study of which he is en^ngi-d; and the accuracy of
the operation will of couree be proportioned to the correctness of
the standard used, and the care with which it is applied.
The instruments employed in microscopic micrometry are of two
kinds, the measurement bein^ taken in one by the rotation of a
fine screw with n divided mified head, whilst in the other a slip
of glass ruled with lines at fixed distances gives a scale which forms
R basis of computation. Each of these has its advantages and tts
disadvantages.
The stage- micrometer constructed by Frauenhofer was formerly
much used by Continental microscopists, and has the advantage of
inJicating the actual dimensions of tl»e objects to be measured;
but it has tho two special disadvantages that a sufficiently small
value cannot be conveniently given to its divisions, and that any "
error in its construction and working is augmented by the whole
magnifying power employed. This instnimcnt has now, however,
almost entirely given place to one of those to be next described.
The screw-micrometer ordinarily used in astronomical measure-
ments (see«Micr.OMETER) can be adnptiil to the cyc-piecc of the j
microsco^w in a manner essentially the same as that in wliich it is /
applied to tlte telescope, — its two parallel threads — of which one is-j
fixed and the other ma.le to approach towards or recede from tliis I
by the turning of the scrcw-^-being placed in the focus of the eye- 1
glass, and being tlicrefore seen as lines crossing its field of view. |
The object is so focusscd that its ima^e is formed in the same plane ; I
and, the latter being brought into such a position that one of its ends I
or margins lies in optical contact with tlic fixed line, the screw is I
turnctl so as to bring the movable line into the like coincidence j
with' the other. But the distance between the lines, as given by the !
number of divisions of the micrometer, will hei-c be the measure-
ment, not of the object itself, but of its magnilied image ; and the t
v.Muje of these divisions, tlicrefore, will dci>end niwn the amplifica-
tion given by tho particular objective used. Thus, snpi>osc each i
division of the micrometer to have an actual value of rTijnjth of an
inch, and tho visual image to have one hundred times the linear
dimensions of the object, the theoretical micromctric value of each I
division would be y^th of xsiirsth, or one-millionth, of an inch, —
a degree of minuteness, however, not practically attainable. It is I
necessary, moreover, to determine the micronu-tric value of the j
divisions of the micrometer, not only for every objective, but foe J
variations in the conditions under which that objective may be i
employed, as reganls the length of tho tube or "body'* of the i
mit-roscope, whicii is varictl not only by tlie draw-tube, .but also, j
in many rases, in the working of the fine adjustment or .slow i
frtotion, and also, in tho case of tho largo-angled powers furnished
tvith adjustment for thicknesa.or the covering-glass, for the degree i
of separation of the front- from the back-glisses of the objective, \
i^U'lt makes a veiy* sensible difference in its magnifying power.
This determination is m.idc by means of a divided glass stage-
micrometer put in the placeof the object, so that the lines ruled \\\mn
it at fixcil intervals shnll be projccte^l ujwn the fichl of vicw^ Tlio
stage-micrometer is usually ruled either to lOOOths of an iDch or
lOOths of a millimetre ; and it is convenient thai one of the dirisions
of its image should be made to coincide exactly with a certain number
of divisions of the screw-micrometer. This may be done by lengtheB-
ing the draw-tube, so as to increase the amplification of the scale
until coincidence has been reached; and the exact amount of this
lengthening should be noted, — as should also the precise positioo
of the milled head of the slow motion (if it acts on the objective,
instead of on the body as a whole), and of the adjusting screw-collar
of the objective itself. Thus, if two lines of the stage-micrometer
separated by 1000th of an inch be brought into coincidence with
the two threads of the eye-piece micrometer, separated by forty
divisions of the screw milled head, the value of each of those divi-
sions is rrhnith of an inch. If tKe above conditions be precisely
recorded for each objective used in micrometry, the micromctric
value of the divisions remains the same for that objective, whenerer
it is employed under the same conditions.
The errors to which micrometers are subject arise (1) from in-
equalities in the ruling of the stage-micrometer, (2) from irregulari-
ties iu the screw of the eye-piece micrometer, (3) from " lost time '*
in its working, and (4) from the thickness of its threads. In order
to eliminate the first and second, it is well to determine the rela-
tion of tho divisions of the two micromctera by the comparison of
a considerable number of both ; the third proceeds from an imper-
fection of workmanship which, if it shows itself sensibly, entirely
destroys the value of the instnrment, while the fourth can be
rectified by the exercise of skill and judgment on the part of the
observer. For, if the micrometer is so constructed as to read zero
when one thread lies exactly upon the other, its divisions indicate
tlie distance between the axes of these threads when separated ; and
the dimensions of any object (such as a blood-corpuscle) lying
between their borders will obviously be too gieat by half the thick-
ness of the two threads, that is, by the entire thickness of one
thread. When, on the other hand, the measurement is being made
(ns of tho distances of tho strife on diatoms) by the coincidence
between certain lines oo the object and the axes of the threads o(
the micrometer, the dimensions indicated by the divisions of the
screw milled-head will be correct.
The costliness of a well-constructed acrew-micrometer being a
formidable obstacle to its general use, a 6im7)ler method (devis^ by
Mr George Jackson) is more commonly adopted, which consists iu
the insertion of a ruled-glass scale into the focus of an ordinary
Huygenian eye-piece, so that its lines are projected on the field of
view. This scale (ruled, like an ordinary measure, with every fifth
line long, and every tenth line double the length of the fifth) is
fixed in a brass inner frame, that has a sliglit motion in the direc-
tion of its length within an outer frame; and this last, being intro-
duced through a pair of slits into the eye-piece just above the
diaphragm, and being made to occupy the centre of the field, is
brouglit exactly into focus by unscrewing the eye-glass as far as
may be requisite. "When the image of the object to be measured is
brought by the focal adjustment of the object-glass into the same
plane, a small pushing-screw at the end of the micronicter (whrae
action is antagonized by a spring at the other end) is turned until
one of the long divisions of the scale is brought into optical contact
with oue edge of the image of the object to be measured, and the
number of divisions is then counted to its other edge, — the operation
being exactly that of laying a rule across the real object if enlarged
to the size of its image. The micrometric value of each division of
this eye-piece scale must be carefully ascertained for each objective,
as in the case of the screw -micrometer, the error arising from in-
equality of its divisions being eliminated as far as jiossible by taking
an average of several. The principal point of inferiority in this
form of micrometer is that, as its divisions cannot be made of
nearly so small a value as those of the screw-micrometer, an
estimate of fractional parts of them often becomes necessary, which
is objectionable as involving an additional source of error. To meet
this objection, Hartnack has introduced the diagonal scale nscd in
mathematical instruments before the invention of the vernier.
Another mode of making micromctric measurements, which forj
some purposes has considerable advantages, is to employ a stages
micrometer in combination with some form of camera Incida
attached to the eye-piece of the microscope, so that the image of
its divisions may be projected upon the same surface as that on
which tho image of the object is throwu. " By first using the niled
stige-miorometcr, and marking on the paper the average distance
of its lines as seen in the centml part of the field, and then ruling
the paper accordingly, the micrometric value of the divisions s*
l>roji'cted may be exactly dotevmined for the objective employed and
the distance of the drawing-plane from the eye-piece, — so that, when
tho image of any object is projected under the same conditions, tlie
dimensions of that image or of any parts of it can be exactly measured
upon the divided scale previously projected, and the true dimen-
sions of the object thus easily ascertained. If, for example, the
lines of a stngc-micromctcr ruled to the thousandth of an inch
should, when thus projecied, fall at a distance of an inch apftr^
then the application of nn oixlinarj" scale of inches (divided into
tculhs) to tU« image of au object p'rojected by tho same objectiTO
278
M I D — M I D
and on the eame nlane wonid give its real dimcDBione in
thousandths of an inch, while the tenths of the inch scale would
represent a real dimension of as many ten-thousandths. It is often
desirable to make such measurements from careful tracing of the
outlines of objects, rather than from the visual images, — this plan
being especiallj' ajvantaf^eous when the exact diracnsions of many
similar objects have to be compared, as iu the case of blood-cor-
puscles, precise measurements of which are not un frequently required
in judicial inquiries. It was by the use of this method that the
late Mr Gulliver made his admirable scries of measurements of the
average and extreme dimensions of the blood-corpuscles of different
animals. .4jid more recently Jlr Dallinger has shown, —by first
malting a very fine camera Inrida tracing of BaeUHvm («nn»
under an amplification of 2000 diameters, and measuring the breadth
of its body in the mode above indicated (which gave it as jjl-ffTjth
of an inch), aud theu by magnifying his tracing from five to ten
diametei-s, and comjiaring, by means of the screw-micrometer, the
breadth of the flagellum wHh that of the body (which last proved
to be just ten times rs gicat), — that, although the theoretical llmik
of resolving power for closely approximated lines is iirjVjuth of an
inch, a semitransparent filament whose breadth is not greater than
Tirir\nnjth of an inch may be clearly discerned, and even measured
with a close approximation to accuracy {Jour, of Royal Micros,
Society, vol L, 1879, p. 169). (W. R C.)
MIDAS, king of Phrygia, is one of those half-legendary
heroes in whom religious legends have gathered round a
real person. The name Midas the king, MIAAI /ANAKTEI,
occurs on a very ancient tomb in the valley of the Sangarius,
the legendary seat of the Phrygian kingdom (Iliad iii.
189). The Phrygian ^nonarchy was destroyed by the
Cimmerians about 670 B.C., and the last king Midas com-
mitted suicide by drinking bull's blood. The name Midas
became in Greek tradition the representative of this ancient
dynasty, but all that is told of him is religious myth. He
is a figure in the cycle of Cybele legends, the son of the
goddess and her first priest. He is also closely connected
witi the cultus of Dionysus, like the two heroic personages
Marsyas and Silenus. The Midas legend was known on
Mount Bermius in Macedonia, and must at one time have
existed in Greece ; two cities Midea, in ArgoLis aud in
Boeotia, recall tlie Phrygian city Midaeium.
See Herod, viii. 13S; Xen., Anab., i. 2, 13; Paus. i. 45, &c
MIDDELBURG, iu Holland, the ancient capital of the
province of Zealand, situated in the middle of the island
of Walcheren, is mentioned as early as 1153, and receives
the title "town" in a charter granted it in 1227. It has
all the characteristics of an old and worn-out place. The
population (2.5,000 in 1739) had sunk to 12,000 or 13,000
by the beginning of the 19th century, and has only begun
recently to increase again, being 15,939 in 1882. The
dwelling-houses, which in 1739 were about 3800, are now
but 3000, and of these about 600 are unoccupied. The
vast warehouses and imposing mansions once belonging to
wealthy families, which have either died out or left the
place, call up the memory of that iirosperity which Middel-
burg enjoyed before its extensive trade, with the East and
West IncUe-s, with England and Flanders, was ruined by
the war with England and the French occupation. By
the opening of the railway (1872) and of the ship canal
(1873) to Flushing Middelburg was lifted out of its isola-
tion, and, with the assistance of the chamber of commerce,
manufacturing industries (iron, machinery, furniture, oil,
cigars, ic.) were established ; but the prosperity anticipated
for Flushing, and consequently for Jliddelburg, remains
unrealized. One of the chief sights of Middelburg is the
splendid' town-hou.se, for the most part erected in 1512-13,
with its front gable adorned with twenty-five statues of
counts and countesses of Holland and Zealand ; it contains
the archives, and a most valuable antiquarian and historical
collection. The abbey, begun in 1150, has frequently been
the residence of royal visitors (Maximilian, Philip the Fair,
Charles V., and so on down to Napoleon I., and William I.,
II., and III.) ; part of it is now an hotel, and part of it is
occupied by the provincial authorities. The great hall of
the building, in which the states of Zealand assemble, is
adorned with beautiful tapestries by Jan de Maecht, repre-
senting the heroic feats of the men of Zealand in the
contest with Spain. What was formerly the nave of the
abbey church is now the New Church, and the ancient choir
constitutes the Choir Church. The former contains a fine
pulpit resting on an eagle, the monument of William, king
of the Romans (d. 1256), and the tombs of Jan and
Cornells Evertsen, two naval heroes who fell in the war
against England in 1666; the latter has the monuments
of the learned Hadrian Junius and of Jan Pieterszoon.
The pro^^ncial court, the corn exchange, the Hof St Joris
and the Hof St Sebastian (formerly buildings belonging to
the guilds of archers, and now places of amusement) deserve
mention. The great museum of Zealand antiquities, col-
lected by the Zealand Society of Arts and Sciences (founded
at Flushing in 1769 and transferred to Middelburg in
1801), shows that the town is the intellectual centre of the
province.
The principal facts in the history of Middelburg are the sieges by
the Flemings in 1288, 129», and 1303 (the last resulting in the
Cfiptnre of tlie town by Guy of Dampierre); the recovery of the
town from the Spaniards in 1574, after an iuvestmeut of nearly two
years; the frequent disturbances among the townsfolk in the 17th
and 18th centuries; the surrender to the English iu 1809 ; and the
arrival and departure of the French in 1809 aud 1814.
MIDDLEBOROUGH, a town of the United States in
Plymouth county, Massachusetts, 34 miles south of Boston.
It has a handsome town-hall and a public library, manufac-
tures woollen goods, straw goods, shovels, shoes, cairiagea,
<tc., and in 1880 had 5237 inhabitants.
MIDDLESBROUGH, situated near the mouth of the
Tees, on its south bank, in the North Riding of Yorkshire,
has now become the principal seat of the English iron
trade. It is a municipal and parliamentary borough,
locally governed by a mayor and corporation, and returns
a member to parliament, The earlier history ef the place
is meagre. Where Middlesbrough now stands (Graves's
History of Cleveland) there were at one time a small chapel
and priory founded by Robert de Brus of Skelton Castle.
These were dedicated to St Hilda, and with some lands
were given by De Brus to the abbey of St Hilda at WhitViy
in 1130. The priory fell into ruins at the time of the
Reformation, and no trace now remains beyond some stones
built into the wall of a brewery. The mayor's chair also
is made from a fragment. In 1801 there were upon the
site of Middlesbrough only four farm-houses. In 1829 a
company styling itself the iliddlesbrough Owners bought
500 acres of land, and commenced building the town. In
1830 the Stockton and Darlington Railway was extended
from Stockton to Middlesbrough ; four years later the town
was lighted with gas ; and after six years more a publie
market was established. The census of 1831 showed the
population to be 154; that of 1841 showed 5709. In
1842 the opening of the docks gave additional importance
to the town. First containing an area of 9 acres, they
were extended in 1872 to 12 acres, with 1700 feet of
quays. Vessels of 3000 tons burden can be accommodated.
From the year 1851, when J. Yaughan discovered the
presence of ironstone in the Eston Hills, the town advanced
with rapid strides. When the jubilee of the town was held
in 1881 (a year late) the population had risen to 55,934,
the area to 2731 acres, and the rateable value to jE140,000,
the population of the parliamentary borough (area 4715
acres) being 72,145. . In the district the-^ are upwards of
M I D— M I D
279
130 blast furnaces, besides large iron and steel works; and
the Thomas-Gilchrist process of making steel proipises for
Middlesbrough importance in the future as a steel entre-
p5t. The make of pig-iron in 1880 was 1,991,032 tons.
There are also shipbuilding, potteries, chemical works, and
a salt trade. Middlesbrough is well laid out, nearly all
the streets lying at right angles to one another. Many of
the churches and the exchange are handsome buildings,
while the station of the North Eastern Railway is probably
the finest in ihe north of England, A splendid park of 72
acres, the gift of the late H. F. W. Bolckow, adds greatly
to the amenity uf the town.
MIDDLESEX, an inland county in the south-east of
England, lying between 51° 25' and 51° 40' N. lat., and
between 0° and 0° 36' W. long. On the south it is divided
from Surrey and Kent by the Thames, on the east from
Easex by the Lea, on the west from Buckinghamshire by the
Colne, and on the north from Hertfordshire by a partly
artificijl and very irregular line. Although with the ex-
ception of Rutland it is the smallest county in England,
its population is exceeded by that of Lancashire only. Its
total area is 181,317 acres, of which 2592 acres are common
or waste lands. The longest straight line that can be
drawn in the county is one of nearly 28 miles from the
north-eastei n extremity near AValthani Abbey to the south-
western at Staines. From north to south in the broadest
part the distance is about 15 miles.
Surface and Geology. — The greater portion of the county
is flat/ although there are sufficient undulations to allow of
a proper drainage of the land. A range of hills runs along
the Hertfordshire border by Barnet, Elstree, Stanraore, and
Pinner, averaging 400 feet in height; another range occupies
the ground just north of London by Hornsey, Highgate,
and Hampstead ; Harrow occupies an isolated eminence
i)etween the two ranges.
The county lies entirely within the basin of the Thames,
and the London CUy extends over a large portion of the
surface. This formation stretches from the mouth of the
estuary of the Thames to the neighbourhood of Marl-
borough. It attains its greatest breadth (little short of 30
miles) in the neighbourhood of London, and e.xtends north-
ward until it is lost beneath the drift of Suffolk and
Norfolk. The following is a table of the various beds of
rock which occur at the surface, with their greatest thick-
acss (in feet) in the district : —
Alluvium (recent river deposits) 15
Posl-Plixcnc TcrtiarUs.
Post-glaci.nI bejs (luick-caitli, gmvrl, it) 50
Glacial drift (boulJcr clay, gravel, ic.) 80
Eoctiic Tdlinria.
Lower Bagsliot sands 100
Loudon Cl.iy <20
AVoolwicli and lUading bods. 90
Ci-'liccoiis.
CImlk nitli ninta . 800
Chalk comes to the surface in ao very few places that it
isscarcot)- worth mention. It is seen near Hareficld and on
the north-west side of South Minims. The depth from the
BOrfaci' to the chalk varies greatly in different parts of the
rountN . This has been proved by the borings for wells ;
thus at Isleworth the depth is 400 feet and at Hampstead
878, while at Kui>-lip it is 7G feet and at Pinner only GO.
The rtcading beds (plastic clays) are brought to the sur-
face at Windsor. Tlicy follow roughly the course of the
liver Colnc from the north of Uxbridge along the flank of
the hills north-eastward, but arc sometimes cut back south-
ward along small side valleys. An outlying mass is
•tjiosed at Pinner. The Bagshot sands, consisting of
gravel and sand permeable to water, once stretched over
the whole extent of the London Clay, but they are now to
be found only on the high grounds at Hampstead, High-
gate, and Harrow. A comer of the main mass enters the
south-west corner of the county near Littleton. Beds of
brick-earth occur in the drift between West Drayton and
Uxbridge.
Several deep borings in the London basin prove the
existence beneath the chalk of beds which do not crop out
in Middlesex. Three of these are in the county; and the
most interesting is that at Jleux's Brewery, Tottenham
Court Road (about 1146 feet), which passes through ♦!»•
following formations : — gravel and clay, 21 feet; Londou
Clay, 64 feet; Reading beds, 51 feet; Thanet sand, 21 feet;
chalk, 655 feet ; Upper Greensand, 28 feet ; gault, 160
feet ; Lower Greensand, 64 feet ; Devonian, 80 feet.
Rivers and Canals. — The Thames is very tortuous in the
44 miles of its course from Staines to Blackwall, and makes
a remarkable bend at the eastern limit of the county where
it forms the so-called Isle of Dogs. The width at Staines
is 200 feet, at Chiswick opposite Barnes 340 feet,- at
Hammersmith 525 feet, at Fulham 820 feet, at Westmin-
ster Bridge 1 100 feet, but at London Bridge it is less than
800 feet ; above the junction of the Lea at the Isle of Dogs
the width is 1350 feet. The ordinary rise of the tide at
London Bridge is 16 feet, and the tide- way ends at Tea-
dington. The port of London begins below London Bridge,
and the channel for from 2 to 3 miles is called the Pool.
The Colne from Hertfordshire enters Middlesex at the
north-western corner of the county. It then runs south,
joining the Thames at Staines, and in its course divides
Middlesex from Buckinghamshire for 15 miles. After the
river leaves Uxbridge it divides out into several small
channels. The Lea from Hertfordshire enters Middlesex
at the north-eastern corner of the county near Waltham
Abbey. It runs south, dividing Jliddlesex from Essex for
15 miles, and falls into the Thames at Bow Creek. Several
branches flow off from the river during its course. The
Brent from Hertfordshire enters Jliddlesex near Finchley.
i It takes a circuitous direction southward through the
1 middle of the county by Hendon, Kingsbury, Tnyford,
Greenford, and Hanwell to the town of Brentford, where it
, unites with the Thames. Wliere the river crosses the Edge-
; ware Road (about 3 miles south of the town of Edgeware)
it is expanded by artificial means into an extensive reser-
voir. The Cran (or Yedding Brook) rises in the district
between Harrow and Pinner and flows under Cranford
Bridge; it crosses Hounslow Heath, and bends round to
Twickenham and Isleworth, where in a divided stream it
falls into the Thames.
There were several other small streams in the neighbour-
hood of London which have left their mark iu the names
of places, but which are now merely sewers, such as the
AVallbrook, the Westbourn, the Tyburn, the Fleet river,
ifcc. The last-mentioned, which runs into the Thames near
Blackfiiars Bridge, was formerly navigable as far aa
Holborn Bridge ; but, the Fleet Ditcii, as it was then called,
having become in the last century a dangerous nuisance,
the lord mayor and citizens were empowered by Act of
Parliament to arch it over. The work was commenced in
1734, and in 1737 Fleet market, occupying the site of the
space i\o\\\ Holborn Bridge to Fleet Bridge, was opened to
the public. The New River, an artificial water-course con-
structed by Sir Hugh Myddelton in the reign of James L
to suiiply London with water, runs through the county from
north to south a little to the west of the river Lea. It
derives its waters from the springs of Amwell and L'hadweU,
increased by a cut from the Lea, in the neighbourhood of
Ware, and enters Middlesex from Hertfordshire about 2
miles north of Enfield. It passes Enfield, Tottenham,
Hornsey, and Stoke Xewington, and is received into the
reservoir in Cleikenwell known as the New River Head.
The Grand Junction Canal leaves llic Thames at Brent-
280
MIDDLESEX
ford, proceeds in a westerly direction by way of Hanwell
and Cranford to West Drayton ; thence iu a northerly
direction it foUowB tho valley of the Colne. It passes
Uxbridge, and after leaving the county takes its further
course by Rickmansworth through Hertfordshire. The
Paddington Canal leaves the Grand Junction Canal at
Cranford, and passes Northolt, Apperton, Tnyford (where
it is carried over the Brent by an aqueduct), and Kensal
Green. At Paddington it joins the Regent's Canal, which
passes the north of Regent's Park, and after proceeding
through the eastern portions of London joins the Thames
at Limehouse. The Regent's Canal is joined to the river
Lea by means of Sir George Duckett's Canal, and thus
there is a through communication from the north-eastern
corner of the county to the south-eastern corner, thence
from east to west, and northward to the north-west corner.
ClimcUe, Soil, Affriculture, He- — The climate of the
county is equable and good, and the shelter of the northern
Lills makes the air mild. Highgate, Hampstead, and
soma other parts are supposed to be specially healthy, and
are recommended for invalids by the medical profession.
The heavy poor clay in the north and north-western por-
tion of Middlesex is chiefly covered with permanent grass.
In some parts it has been made fit for arable cultivation
by the addition of chalk, lime, and ashes. The rich
deposits from the Thames have formed a soil which when
well manured is specially suitable for market gardens.
From its nearness to London the district l^as long been
famous for high farming, and the divisions devoted to
different kinds of farming are well marked. The greater
part of Gore and Ossulston hundreds, portions of Spel-
thome and Edmonton hundreds, and a strip do'wn the
western side of Elthorne hundred are devoted to meadow
ajid pasture. The arable land is chiefly found on the
western side, and between the Great Western Railway and
the Thames. It is also to be seen in the north-western
district. With the constant increase of London, houses
have encroached upon the fields, and most of the market
gardens w-hich were situated in the neighbourhood of
Islington and Hackney have disappeared. The strip of
land by the Thames from Brentford to Chelsea was given
np almost entirely to market gardens, but Fulham is fast
being built over.
According to tho returns for 1882, tne area occupied by grain
and (^een crops, grass, &c., was 118,470 acres. Of this amount,
16,337 acres weie under corn crops (wheat, 6410; bailey, 3083;
o.its, 3S95; and beans and pease, 2636); 13,451 under green crops
(including potatoes, 3019; turnips, 1539; mangolds, 1692; cabbage,
fco., 118S); 3025 under clover and grasses sown in rotation ; and
82,782 under permanent pasture. Orchards occupied 3419 acres;
market gardens, 6900; nursery grounds, 447; aud woods, 2382.
In the same year the horses numbered 6939 (4188 used for agri-
cultural purposes); cattle, 23,283 (cows, 15,390); sheep, 23,916;
and pigs, 12,035.
The following wore the landowners in the county (exclusive of
London) at tho time of the Domesday survey; — the king, the arch-
bisliop of Canterbury, the bisliop aud canons of London, the abbeys
of Westminster aud Holy Trinity at Caen, the nunnery of Barl<iii£;,
the Earls Roger and Morton, Geoffrey de Mannevole, Ernulf tie
Hesdiug, ■Walter Fitz Otlier, Walter de St Wnlery, Richard Fitz
Gilbert, Robert Gcrnon, Robert Fafiton, Robert Fitz Roselin,
Robert Blund, Roger de Ramcs, William Fitz Ansculf, Edmund do
Salisbury, Aubrey de Vore, Ranulf Fitz Ilger, Derman, Countess
Jiulitb, and the king's almoners.
In 1873, according to tho neturn of Oimifra of Lnnd, tho total
nnmber of owners in the county (also exclusive of London) was
11,881, of whom 9006 owned loss than an acre. Tlie extent ot
lands (including common or waste lands) is given as 145,605. The
gross estimated rental was £1,611,655. Sixteen owners each j'os-
uessed over 1000 acres. Tho crown owned 2382 acres (annual
value £5503); the duchy of Lancaster, 2273 acres (£4492) ; Ecclesi-
astical Commissioners, 1308 acres (£46.619) ; All Souls' College,
Oxford, 1813 acres (£4724); Christ Church, Oxford, 1132 acres
(£1635) ; and King's College, Cambridge, lOi'7 (£1084).
Many villages of Middlesex, cs[)ecial!y those near to
London, were formerly famous for their mineral springs.
Some pkces are still supplied with water froB wella ; bni
the Bamet, the East Middlesex, the Grand Junction, the
West Middlesex, and the New River Water Compamea
serve a large part of the county.
itannfactures aTid Trade. — "There is little to remark with
regard to the manufactures of the ctWnty outside of London.
Brick-making and tile-making have always flourished, and
malting, distilling, and soap-making are favourite industrieat'
Gunpowder mills e.xist at Twickenham and Bedfonti
The market-towns for com are Uxbridge, Brentford, and
Staines, for cattle and sheep SouthalL A horse and cattle
fair is held at South Mimms and Bamet.
Railvxiys and Moods. — As London is the centre of the rail va J
system of England, it is evident that many of the lines most itm
through Middlesex. For similar reasons it is well provided with
roads.
Population.— TVa total population of Middlesex was 2,639,765 in
1871 and 2,920,485 in 1881, or excluding the seven metropolitan
boroughs lying within the county 276,028 in 1871 and 394,089
in 1881. Most of the towns and villages have largely increased
during the period between 1871 and 1881 ; the populations of Acton
and 'Tottenham have more than doubled, and Chiswick, Ealing,'
Edmonton, and Willesden have almost doubled. Of the larg«r
places the least increase has been at Brentford, which numbered
10,271 in 1871, and reached 11,808 in 1881. At the time of tho
Domesday survey the population of Middlesex, exclusive of LoDdon,1
was 2302.
Qorcrnmtnt. — Unlike other counties, Middlesex has no high^
sheriff api»intod by the sovereign. It is subject to the City of
London, and one of the sheriffs appointed by the lord mayor'is sheriff
for Middlesex. When Henry I. came to the throne be gave the city
an extensive charter, and one of the privileges either granted or
confirmed by the king was the perpetual sheriffwick of ilidillesex. ]
The whole of the county is included in the diocese of Loudon,
and is divided between the archdeaconries of London and Middlesex.
When Henry VII 1. created the bishopric of Westminster he allotei
the whole county (the parish of Fulham alone excepted) for its
diocese. Edward VI., however, dissolved the bishopric in tha
fourth year of his reign
Tlie county is divided into six hundreds, which remain the sarae
as they were at the time of the Domesday survey, except that lUo
name of one has been changed: — Ossulston (Osulvestane U. ), Eilmon.'
ton (Delmetoue D.), Gore (Gara D.), Elthomo (Helctome oi
Heletlioruo D.), Spelthorno (Spelotome or Spelethorne D. ), laW
worth (Honeslaw D., i.e., Houoslow). The division into hundreds'
is now merely a name, and a record of a former system of local
government.
There are thirty-two poor-law unions, but the tiniona bdyond'
London are only eight in number, viz., Brentford, Edmonton^'
Fulham, Hackney, Hampstead, Hendon, Staines, Uxbridge.
The majority of hospitals are in London, but there is a traininf
hospital at Tottenham, St John's Hospital at Twickenham, and
cottage hospitals at Enfield, Ealing, Hayes, Hillingdon, Sudbury,
and Teddiugton. The Royal India Lunatic Asylum is at Ealing,'
and the two county asylums at Colney Hatfh and Hanwelh
The county is within the jurisdiction of the central criminal cour
and alsoof the metropolitau i)oIice(with the exception of the City)
Parliamentary Ktprisentati0n. —There are nine constrtuencies it.'
Middlesex, returning nineteen members, viz., two for tho county/
four for the City of London, two for each of the boroughs of Weat-
niiuster, Finsbury, MaiyJfl>ouc, tho Tower Hamlets, Chelsea, and
Hackney, with one for the university of Loudon.
In tho parliament of 1295 Middlesex was represeiited by two
members ; in 1298 London sent two members as w ell as the countj".
For the parliament of 13'20 and subsequent parliaments London
elected four n>cmbers, but it does not appear that all wi-rc allowed
to sit. From the 16th century, however, the city has always sent
four members to parliament. In 1547 Westminster first sent hrr
two members, and from that time until 1832 the only seats were
those for the county and the two boroughs. In 1832 the boroughs of
Finsbury, Marylebouc, and Tower Haniletswere adde<l, and in 1866
the boroughs oi^ Chelsea and Hackney and the university of London.
History.— The district now included in Middlesex was largely
occupied by forest up to a comparatively recent period, and its
population must always have been very sparse. A few prehistoric
remains have been discovered at various times, — bones of the
elephant, hippopotiimus, deer, 4c., at Old Brentford, elk horns
near Chelsea Hospital, fosail teeth, fish, fruit, ic, at Highgate,'
and quite recently, in 1879, while tho foundations wore being dug
out for Drunimond's New Bank fit Charing Cross, a large number
of prehistoric animal remains. Flint instruments have also been'
found to cover a considerable area. During the Cvitish period the
district is supposed to have been Inhabited by the Trinobantcs, bnt
VOL. XVI
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PLATE III
MIDDLESEX
28 J
the Ut« Dr Onest affirms th&t the valley of the Lea was the \7estern
boaDdary of that tribe. In answer to the question — What became
of the district between the Lea and the Brent t this great authority
■tates that the district was merely a march of the " CatuvcUanni,"
• oommon through which ran a wide trackway, but in which was
neither town, village, nor inhabited house. Dr Guest also declares
that the boundaries of the Catuvellaunian state, a central kingcfom
formed or m'uch extended by Cassivellaunus, can be traced in part
along the northern limit of Middlesex by following an earthwork
called Grimesditch "from Brockley Hill to the woodland of the
Colne Valley and thence to the Brent, and down the Brent to the
Thames."' Some earthworks and encampments stili exist vhich
are attributed to the Britons.
When the country was under Roman rule great improvements,
due to the growing importance of Londinium, were made in this
district Several roads in connexion with the city must have been
constructed, more especially the great northern and eastern roads,
Dr Guest do^ not be-lieve that the present Watling Street could
have had any connexion with the Watling Street which came down
the Edgeware Roed, passed along by Park Lane, and crossed the
Thames at Westminster. In the Antonine Itinerary mention is
made of three stations, viz., Londinium, SuUoniacse, and Pontes.
Salloniacae is now Brockley Hill ; Pontes is supposed by Stukeley
to mean Staines, but Horsley held that it was intended for Old
Windsor, and others supported the claims of Colnbrook and Long-
ford. Roman camps have been found in many parts of the county,
and Dr Stukeley supposed that the Brill, near St Pancras, was the
site of the battle between Boadicea and the Roman legions which has
left a slight record in the name of Battle Bridge. The Roman
remains found at different times are too numerous to mention here
in detail. Coins, urns, and tiles were found at EuGeld, a sepulchral
urn at Hampstead, and numerous gold coins and ornaments at
Bentley Priorj-, Great Stanmore, in 1781.
Cowey Stakes, about a furlong west of Waicon Bridge, is supposed
to bo the locality of the ford by which Julius Ctesar crossed the
Thames. Cfesar makes special mention of the sharp stakes which
he had to encounter, and Bede says that the remains of the stakes
were to bo seen in his day. Camdeu was the 6rst to fix upon this
as the spot where Csesar crossed, and he is supported by Dr Guest,
but the identification is not undisputed. Although a ford existed
here as late as 1807, and stakes were found up to the end of the
18th century, it has been affirmed that they were placed in their
position with another object than to oppose an enemy's progress.
Roman remains have been found at Shepperton near Halliford, at
the Middlesex end of the ford. A vase was dug up in 1817, and
the remains of a Roman cemetery have also been discovered.
As to the earliest Saxon occupation we are left very much to con-
jecture, and the name itself is somewhat of a puzzle. It is evident
that no tribe could have obtained the name of Middle Saxons until
after the settlement of the districts on each side of it by the East
and the West S.axons. As Middlesex was for a period dependent
upon the kingdom of Essex, it is probable that the name did not
come into use until London had become a Saxon city, although there
is reason to'- believe that previously Saxon settlements had been
made on several places by the river and elsewhere. Bede tells us
diat London was in the hands of King Seeberct in 60<, and was then
the chief town of Essex. Just a century afterwards— that is, in 704
— the king of the East Saxons granted away land at Twickenham,
showing that Middlesex was then dependept upon Essex. It is
worthy of note that the two districts now forming the counties
in which London and Southwark are situated were separated
from the kingdoms to which they originally belonged probably
on account of tlie importance of the city of London and the borough
of Southwark, Middlesex from the kingdom of Essex and Surrey
or the South Ridge (A.-S. Su«-rige) from the kingdom of Kent
Middlesex appears never to have been independent. The admini-
strative shire was let to the men of London and their heirs to be
held in farm of the king and his heirs, and "the subject shire has
to submit to the authority of the sherifls chosen by the ruling
city." •
Middlesex is only once mentioned in the Saxon Chronicle, under
date 1011, where it is noticed as one of the districts overrun by
the Danes. One manuscript (A. Winchester) mentions the Middle
Saxons as receiving the true faith under their alderman Peada
in 663 ; but this is evidently a mistake of tho scribe, for the fact is
taken from Bede, and ha writes Middle Angles, as do the other
MSS. of the Chronicle.*
' -Lecture em the Orlltin o( London," Athrnmrt, IMS, No. 2032.
" Frteman, Sorman Comjuett, rol v. (1876) p. 46S.
» \u ttie above passage from the Chronicle, where (ho dlitrlcts oremin by the
Dmn In toil iAt- enumerated, the nhhei, which look Uielr nnmcj from their
eWcf townl, Qrt dUtinctly marked off from the dlatrkts which took their namei
troiB tho peoples who Inhabited them. Of the latter there are, bf«l<te! the
Ulddle Saxons, tiio East Angl. », the Kentlngs, and the South Sasons. lllddleocr
la atylcd an admlnlstrolivc sliho. because It was not liistorlcally a shire, but
only one for (he purposes of admlnlptratlve organlialion. Of the prevent forty
cotmtks Iwenly^lght are and twelve are not shires. Wcssex was divliled ioto sis
■bins, and Mercla Into eightceD, with the sobactiueat tdOltloti of RatUmd. taken
The Saxons appear to have settled over a large portion of the
district, and for the purpose of settlement they must have made
considerable clearings in the vast forest of Middlesex. There seenu
to be good reason for believing that previous to their coming the
roads passed through waste lands. By the time of Edward the
Confessor a large proportion of the present towns and villages were
in existence. Mr Elton, in his Orighis of English i/wfory,'' mentions
a curious fact with relation to the tenures which prevailed in some
of these places. He alludes to a ring of manors eucircling aucieHt
Loudon where the custom of Borough English or junior nght was
prevalent.' He then goes on to point out that in this cluster of
manors there are several varieties of the custom: — " Its benefit in
Islington and Edmonton was confined to the youngest son ; at
Ealing, Acton, and Isleworth it extended to the brothers and male
collateral heirs ; and in a great number of instances the privilege
was given to females as weS as to males in every degree of lelstion-
ship. These variations are of no very great importance, the custom
being modified in all parts of the country by the rule that special
broof must be given of any extension of that strict form of Borough
English for tho benefit of the younger son of which alone the courts
have cognizance. But it is of the greater interest to observe that
in several places near London ' it is the custom for the land to
descend to the youngest, if it is under a particular value of five
pounds, but if it is worth more, it is parted among all the sons*
{First Real Property Cmnmissi(m Hvidmcc, p. 254)."
The great forest of Middlesex continued long after the Norman'
Conquest, and even as late as the reign of Elizabeth portions of it
still existed quite close to London. Fitz Stephen, the monk at
Canterbury and secretary of Thomas a Becket, mentions in hia
interesting description of London the immense forest with its
densely wooded thickets, and its coverts of game, stags, fallow-
deer, boare, and wild bulls. A few years after Fitz Stephen's death,
in the reign of Henry III. (1218), the forest was disafforested, and
some of the wealthy citizens took tho opportunity of purchasing
land and building upon it. Matthew Pans, in his Ijfe of the twelfth
abbot of St Albans, describes the woods contiguous to the Watling
Street between London and St Albans as almost impenetrable, and
so much infested by outlaws and by beasts of prey tuat the numer-
ous pilgrims who travelled along the Roman road to the shrine of
Albanus were exposed to imminent danger.
There is little further history that can be told of Middlesex.
There are many interesting incidents connected with some of the
places, but corporate life has been crushed out of the county by the
greatness of London. Not a single place except London has grown
into importance, and nowhere outside of London is there a building
of fi ret-late interest. The villages on the Thames early began to
increase in size on account of the convenience of locomotion
supplied by ths river. It is only since the extension of the railway
system that tho villages to the north and north-west of London
have grown in size, and this growth has been mainly due to the
building of houses for the use of the Londoners.
BWttography. — John i^orizn. Speculum Britanntie: the firtt parte, an hUl«ri-
eall and ehorographiealt discription of Middiestjr, 4to, London, 1593, reprinted In
1637 and 1723; John Dowack, The Anttquitiel of iliddleiex, paits 1 and 2, foll(\
London, 1705-6; Ric. Kewcourt, Jteptrtorium Ecctcsiattuum Paroehiale iMn-
dincnte, 2 Tols. folio, London, 1708; Rev. Tliomas Cox, itagna' Britannia tt
Ul^-nia, antiqua el nopa, 6 vols. 4to. London, 1720 (vol. lil. conuins Middlesex);
A DeKrIplion of the County of Uiddlelez, Rvo, London, 1776; Rev. Daniel
Lysoni, The Emironi of London, 4 vols. 4to, London, 1792-96 (vols. 11., Hi., and
supplement, 1811, contain Middlesex); John Jliddietoa, General Yiev of the
Agrieullure of i/iddleux, 4(0. London, 1793: Peter foot, Ceneial Vieu of the
AfruuJIure of Uiddleiez, iU>, LoTtdon, nH ; John Middielon, lieu: of the Agri-
eulture of iiiddlelex, Svo, London, 1798, second edition, 1607 ; Rev. D. LysoQs.
An BUtorUat Account of thou Pariihet in the County of Middletex vhich are not
deteribed in The Enrironi of London, 410, London, 1600 ; O. A. Cooke, ifodern
Britith Traveller. 12mo, London, 1802-10 (vol. xli. contains Middlesex); E.
W. Braylcy, Rev. Joseph Nightingale, and J. Norris Brewer, '-London ami
Middlesex,-' in Beautiei of England and IValei, 5 vols. Svo, London, 1610-16;
Rev. William Bawdwen, A Translation of the Record rolled Domesday so far as
relates to the Counties of lliddlesex, Uerlford, Buctiugham, Ozfoi% and Olouceiter.
4(0, Doncastcr, 1812; other publications conceinlng (he Domesday of Sliddlescx
are facsimile, foiio, Sooihampton, 1861 ; a literal extension of (he Latin text
folio, London, 1662; \Vm. Ryley and Hy. Dethick, The Visitation of Uiddlrscx
begun in 1663, folio, Salisbury, 1820; William PInnock, The History and Topo-
graphy of Uiddiesex, 12mo, London, 1824 (roL 8 of Plnnock's County Bistories);
W. Smith, Delineations of the County of Middlesex, 8ve, London, 1834; Samuel
Tymms, A Compendious Account of Middlesex and London and ^Vellmin^ttr iCasa-
den-s Britannia epitomised and continued, vol. vli,), London, 1843; J. H. Sper-
ling, Church Waits ia Middlesex, being an Ecctesiotogisf s Guide to that County,
12mo. London, 1849: The Beauties of Middlesex, being a particular description of
the principal seats of the nobility and gentry in tlie County of Middlesex, Svo,
Chelsea, 1850; The Counties of England (No. 1, Middlesex). Svo, London, 1855;
Transactions of the London and Middlesex Archteologieat Society. Svo, 1860-82;
James E. Hai-ting. The Birds of Middlesex, Svo, London, 1866 ; Henry Trimca
and W. T. -Thiselton Dyer, Flora of Middlesex, Svo, London, 1869 ; William
Hughes, 27ie Geography of Middletex for the use of schools. 12mo. London, 1872;
William Lawson, Collins' s County Geographies (Middlesex). 8ro. 1872; The
Geography of the Counties of England and Wales (No. 10, Mid.lleaexl, 8vo. Mm-
Chester, 1872 ; W. E. Baxter, The Domesday Book for the County of Middlesex,
being that portion of a Return of Omers of Land in England and Waits in 1873
iehich refers to Middlestx. 4to, Lewes, 1877. (H. B. W.^
(It Is boUeved) from Nortliamptonshlre. Yorkshire was taken from Kortbumbria,
Lancaahire fiom Cumbria, and, Uat of all, Uonmouthshire fioni Walea, by au
Act of Henry Vlll.'a t^iga.
4 Pp. 188-49, and note.
0 Ur Comer i;lre« the number of bistaaccs b« baa found at alxtrcn.
282
il 1 D D L E T O JN
MIDDLETON, a market and manufacturing lovm of
I^ncashire, is situated on the Irk, near tlie Rochdale
Canal, and on the Lancashire and Yorkshire Railway,
about 5 miles north of Manchester and i v'cst of Oldham.
It includes the township of Tonge, an isolated portion of
the parish of Prestwich. The church of St Leonards is an
old structure of mixed architecture, with a low square
tower. The oldest portion of the building dates from the
12th century, but the main portion from 1412, and the
south aisle from 1524. It underwent extensive restoration
in 1869. The Queen Elizabeth Grammar School, a build-
ing in the Tudor style, was founded in 1572. There are
public baths and a free library. The prosperity of the town
dates from the introduction of manufactures at the close of
last century. The staple trade is the spinning and weaving
of cotton, and the other industries include silk weaving,
calico printing, bleaching, dyeing, ironfoundmg, and the
manufacture of soap and chemicals. There are several
collieries in the neighbourhood. The town was at an early
l)eriod in possession of the Bartons, from whom it passed
by marriage in the IGth century to Sir Ralph de Assheton.
The population of the urban sanitary district of Middleton
»nd Tonge in 1881 was 18,952.
MIDDLETON, Conyers (1683-1750), the earliest and
most eminent example of the .spirit of theological rational-
ism in the English Church of the 18th century, was the
son of the rector of Hinderwell near Whitby, and was born
at Richmond in Yorkshire, on December 27 (or, Recording
to another account, on August 3), 1683. He graduated at
Cambridge, took orders, and in 1706 obtained a fellowship,
which he soon resigned iipon contracting an advantageous
marriage. In 1717 a dispute with Bentley, upon an
extortionate demand of the latter on occasion of Middleton's
being created D.D., involved him in an acrimonious con-
troversy, which called forth several pamphlets from his
pen full of powerful invective, and among them his first
^considerable literary performances, the Jiemarks and
'Fuiiker Hemarh on Bentley 's Proposals for a Keiv Edition
cf the Greek Testament (1721). "You have laid Bentley
flat upon his back," wrote Colbatch. " I scorn to read
what the rascal has written," wrote Bentley, — who, how-
ever, only resorted to this affected disdain after a fruitless
attempt to fix the authorship upon Colbatch, but who
might justly have commented upon the impropriety of
Middleton's endeavour to visit his grievances ujjon the text
of the New Testament. Private resentment and uncurbed
[lersonality were throughout his life too frequently the
motive and the note of iliddleton's controversial jmblica-
tions. In 1723 he was involved in a lawsuit by person-
alities against Bentley, which had found their way into
his otherwise judicious tract on library administration,
written on occasion of his appointment to the honourable
office of university librarian. In 1726 he gave great
offence to the medical profession by a dissertation contend-
ing that the healing art among the ancients was only
exercised by slaves or freedmen. Between the dates of
these publications he visited Italy, and made those observa-
tions on the pagan pedigree of Italian superstitions which
he subsequently embodied in his Letter from A'ome (1729).
This cogent tract, wliilo establishing the author's main
'proposition with abundant learning and wit, gave at the
same time the first clear indication of theanti-.sup'^rnatural-
istic bias of his intellect, and probably contriouted to
prepare the storm which broke out against him on his next
publication (1731). In his remonstrance with AVaterland
en occasion of the latter's reply to Tindal's C/tristianily as
Old as the Creation, Middleton takes a line which in his
'day could hardly fail to cxjjose him to the reproach of
infidelity. He gives up the literal truth of (he primeval
Mosaic narratives ; and, in professing to indicate a short
and ea«y method of confuting Tindal, lays principal stress
on the indispensalSleness of Christianity as a mainstay of
social order. This was to resign nearly everything that
divines of the Waterland stamp thought worth defending.'
Middleton was warmly assailed from many quarters, and
retreated with some difficulty under cover of a sheaf of
apologetic pamphlets, and a more regular attendance at
church. A freethinker in the strict sense of the term he
certainly was ; but how far freedom of thought was carried
by him it is not easy to ascertain. His adversaries — some
of them men who gravely maintained that Eg)-ptian
civilization originated in the age of Solomon— were unable
to fix any serious imputation upon him ; on the other hand
it is clear that the natural attitude of his mind towards
supernatural pretensions was one of suspicion, and that his
temperament was by no means devout. That he was
nevertheless not incapable of a disinterested hero-worship
was evinced by his next important publication, the elegant
but partial Life of Cicero (1741), a work which, if far
below the standard of modern exactness, may yet compare
in spirit and execution with the best jjroductions of the
Italian Renaissance. It is, indeed, as remarked by
Forsyth, " rather an historical composition, in which
Cicero is the jirincipal figure, than the portrait of the man
himself"; and Dr Parr has pointed out Middleton's
unacknowledged obligations to the forgotten EcUendenua,
which, however, with the ardour of a discoverer, he seems
to have considerably overrated. The work was undertaken
at the instance of Lord Hervey, in correspondence with
whom also originated his disquisition on The Roman
Senate, published in 1747. The same year and the follow-
ing produced the most important of all his writings, the
Introductory Discourse and the Free Inquiry concerning
the miraculous powers then commonly deemed to have
subsisted in the church after the apostolic age. In com-
bating this belief Middleton indirectly established two pro-
positions of capital importance. He showed that ecclesi-
astical miracles must be accepted or rejected in the mass;
and he distinguished between the authority due to the
early fathers' testimony to the beliefs and practices of their
times and their very .slender credibility as witnesses to
matters of fact. Some individual grudge seems to have
prompted him to expose, in 1750, Bishop Sherlock's
eccentric notions of antediluvian prophecy, which had then
been before the world for a quarter of a century. The
same year he died of a declijie at his seat at Hildesham in
Cambridgeshire, leaving a widow, but no children.
WidJlcton's most ambitious woik is obsoleto from no fault of
his, but his controversial writings retain a permanent place in the
history of opinion. In liis moi-e restricted sphere he iiray not in-
appropriately be compared to Lessing. Like Lcssing's, the diaracter
of his intellect was captious and iconoclastic, but redeemed from
mere negation by a passion for abstract truth, too apt to slumber
until called into activity by some merely personal stimulus. Hia
diction is generally miksculine and harmonious. Pope thought him
and Hookc the only prose writers of the day who deserved to he
cited as authorities on tlie language. Parr, while exposing hia
l)lagiarisnis, heaps encomiums on Lis style. But his best qualities,
his impatience of superstition and disdain of mere external
authority, arc rather moral than literary. As a scholar lie is rather
elegant than j^rofound; as a controversialist he has more vigour than
urbanity, and more wit than humour. He has been unjustly
attacked liotli as nutlior aiid as man by De Quincey, who strangely
accuses his stylo of coUocjuialism, and taxes him with eating tha
church's bread while denving her doctrines. In fact Middleton's
private means were ample, his ecclesiastical emoluments tiitling,
ond his candour obstructed his path to much more considerable pre-
ferment The best general view of his intellectual character end
influence is to bo found in Leslie Stephen's Ent/Iisli Thought in Uu
Eiglilicnth Ceittunj, chap. vi. A handsome edition of his works,
containing several posthumous tracts, but not including the Lift
0/ Cicero, appeared m 1752.
MIDDLETON, TnoM.w (r. 1570-1627), held a leading
place among the dramatists of the reign of James I. His
M I D — M I D
28c
popularity would seem tohave first come to a height about
1607. This is a fair inference from the fact that in this
and the folloiving year a whole swarm of comedies from
his pen were licensed and published — A Trick to Catch the
Old One, The Family of Love, The Phoenix, Michaelmas
Term, Your Five Gallants, A Mad World My Masters.
Only the first of these kept the stage after the author's
own generation, though in point of wit and constructive
skill it is not superior to The Phomix (a serious comedy) or
Tour Five Gallants (a bustling and gaily humorous farcical
comedy). The plot of the Ti-ick bears a family likeness
to that of Massinger's Neio Way to Pay Old Debts; the
titles in fact might be interchanged. A ruined scapegrace
outwits his creditors and a usurious uncle by coming to
town with a courtesan and passing her off as a widow with
a fortune, whom he treats with deferential friendship, but
hardly dares to love, ruined and hopeless as he is. His
uncle lends him money that he may woo in proper state ;
his creditors also intrigue to have the honour of supplying
him with all the needs of fashion ; and the lady receives
many costly presents from aspirants to her hand and
fortune. Though Middleton was apparently not in high
popidarity till 1607, he had made his debut as a satirist
ten years before; and if ilalone is right in his conjecture
that the Mayor of Queensboi-ouffh is identical, with the
JRantlall Earle of Chester mentioned by Henslowe in 1602,
he had done dramatic work of a much higher kind. Like
The Chan^eliny, a later production, in which Middleton
had the assistance of Rowley, the tragedy of the Mayor is
named after a character in the insignificant comic underplot.
Such a title scares away readers weary of half-intelligible
Elizabethan fun and satire; but Simon the comic mayor
is a very subordinate figure in the play, and the tragic
portions alike in situation, characterization, and language
rank among the very noblest productions of the Shake-
spearian age. There are scenes in the Changeling also
which Mr Swinburne, with a judgment that will not be
disputed, assigns to Middleton, unsurpassed for intensity
oi passion and appalling surprises in the whole range of
Elizabi than literature. The execution of these scenes is
I'ar beyond any power that Rowley showed in single-handed
work, but well within the scope of the author of the
Mayor of Queenshorough and Wmnen Beware Women.
This la.st play, in which every one of the characters
important enough to be honoured with a name perishes at
the end in a slaughter so rapid as to be somewhat confus-
ing, was apparently one of Middleton's later works, and
the simple and measured development of the plot in the
first acts seems to show traces of the influence of Massinger.
Middbton's verse, when charged _with the expression of
impassioned love, contains many echoes of the verse of
Romeo and Juliet, as if his ear had been fascinated by it
in his youth. His language generally proclaims him an
admiring disciple of Shakespeare's; and in daring and
happy concentration of imagery, and a certain imperial
confidence in the use of words, he of all the dramatists of
that time is the disciple that comes nearest the master.
The Witch, by which Middleton's name has of late been
linked with Shakespeare's in groundless speculation as
being part author of Macbeth, is by no means one of
Middleton's best plays. The plot is both intricate and
feeble, as if the play had been written with a view to the
half-comic spectacular exhibition of the witches, with their
ribald revelry, their cauldrons, hideous spells, and weird
incantations. Charles Lamb's comparison of Middleton's
witches with Shakespeare's is one of the most exquisite
morsels of criticism ; but, when he says that Middleton's
witches are " in a lesser degree fine creations," he ought
perhaps to have added that they are merely embodiments
of the vulgar superstition, put on the stage to excite
laughter rather than fear among a half-believing audience,
an audience ready to laugh at them in the light and in a
crowded meeting, whatever each might do in the dark
alone. That Middleton had any share in Macbeth ia a
conjecture resting solely on the fact that the opening
words of the song of the witches about the cauldron in
Shakespeare's Macbeth occur alio in the incantations about
a cauldron in the last act of Middleton's Witch, and
that Middleton's song was inserted by Davenant in an
" amended " reproduction of Macbeth. If either borrowed
the words of this song from the other, that is no evidence
of further co-operation ; besides all that is common to the
two was probably as much public property as a nursery
rhyme. There is no evidence as to whether The Witch
appeared before or after Macbeth. Middleton co-operated
with Dekker in the Roariyig Girl ; with Rowley in A Fair
Quarrel, The Spanish Gipsy, and The Changeling; and
with Jonson and Fletcher in The Widow (one of the few
of Middleton's plays reproduced after the Restoration^
Towards the close of his life Middleton got into difficulties
with the privy council from writing a very clever political
play apropos of Prince Charles's unsuccessful wooing of the
Spanish infanta in 1623. The chief personages in Spanish
politics and their manoeuvres were represented with most
ingenious skill in the pieces and movements of A Game at
Chess. This play was stopped by royal authority, and the
prosecution of the author was allowed quietly to dropi
The few animportant facts known in Middleton's private
history are collected in Mr Dyce's admirable edition of his
plays. He enjoyed the office of city chronologer, and was
often employed to write pageants and- masques, in one case
at least contracting for the whole exhibition, besides fur-
nishing, the words. He died in 1627, and was buried at
Newington Butts.
MIDDLETOWN, a city and port of entry of. the
United States, and one of the shire towns of Middlesex
county, Connecticut, lies on the right bank of the Con-
necticut river, about 30 miles from its mouth, directly oppo-
site the well-known Portland quarries, and 24 miles from
New Haven by rail. Built on ground rising gently from
the river, with its principal streets keeping the direction of
the valley, and the cross streets climbing the slope, Jliddle-
town is a place of considerable attractiveness, and the views
from the higher points are particularly fine. Water Street,
with the wharves and shipping. Main Street, with the
commercial houses and hotels, and High Street, with its
mansions and gardens and trees, are the leading lines of
the city. On the high grounds behind stand the handsome
buildings of the Wesleyan (Methodist Episcopal) University.
The institution, mainly organized by Wilbur Fisk, D.D.,
was chartered in 1831. To the two buildings with which
it started have been added Rich Hall, with the library of
about 30,000 volumes, Judd Hall, with scientific collections
of great value, the Memorial Chapel, erected in the
centenary year of American Methodism, and the Observa-
tory HalL Since 1872 the courses of the university have
been open to both sexes. In 1882 the number of pro-
fessors was 20, and of students 191, including 14 females.
The Berkeley Theological School (Main Street), founded
by the Episcopal Church in 1854, had in 1882 7 pro-
fessors and 41 students, with a library of 17,000 volumes.
A hill \\ miles to the south-east of the city is occujiied by
the State General Hospital for the Insane, the principal
building having a frontage of 768 feet, and the grounds
extending to 230"acres; and on another hill to the south-
west of the city stands the State industrial school for girls.
As vessels dra\ving 10 feet of water can reach its wharves,
Middletown carries on a considerable trade by the river. In
1882 1613 vessels, with a burden of 240,000 tons, entered
the port, and 1613 vessels, with a burden of 350,000 tone,
284
M I D — M I D
cleared ; and the Middletewn district owned 83 bailing
Te&sels and 22 steamers. Both the silver and- the lead
mines which were formerly worked in the vicinity have
been abandoned, but cast-iron, britannia, and silver-plated
goods, sewing-machines, pump?, webbing, and tape are
among the local manufactures. The population of the city
increased from 5182 in 1800 to C850 in 1880. First
settled in 1G3C, Middletowu was incorporated as a town in
1654, and as a city in 178i
MIDDLETO^V^r, a manufacturing village of the Tnited
States, in Walllull township. Orange county, New York,
55 miles N.N.W. of New 'Vork, at the junction of four
railroads. It is a clean well built place, in the midst of a
fine dairy-farming and stock-raising district, manufactures
saws, files, felt hats, blankets, agricultural implements,
printers' materials, <tc., and is the seat of the State
Homoeopathic Insane Asylum. The population was 6049
in 1870 and 8494 in 1880.
JIIDHITRST, an ancient parliamentary borough and
market-town of Sussex, is picturesquely situated on a
gentle eminence above the south bank of the AVest Pother,
on three railway lines, 50 miles south-west of London and
13 north from Chichester. The church of St Denis (re-
stored in 1881-83) is chiefly Perpendicular in style, but
the lower part of the embattled tower is probably Norman.
At the grammar school, founded in 1672, Richard Cobden
and Sir Charles Lyell were educated. A new public hall
was opened in 1882. The old castle of the De Bohuns
stood on a mound above the river, now overgromi with
trees. In ancient times a commandery of the Knights of
St John of Jeriisalem had jurisdiction over the district
now forming the liberty of St John. The prosperity of
the town depends chiefly on agriculture. A market is held
weekly, and a fair three times a year. The population of
the parliamentary borough, which has an area of 26,172
acres, was 6753 in 1871, and 7221 in 1881.
llidlmrst is not mentioned in Domcsd.iy, being inclndtd under
Easebourne. lu the reign of Henry 1. it w.is held by the king
M a minor barony. In tlie time of Edward I. it nasscd into
the possession of the De Bohuns. From the time of Edward II.
till 1832 it returned two membcra to parliament, but since then
only one.
MIDIAN was one of the peoples of North Arabia whom
the Hebrews recognized as distant kinsmen, representing
them as sons of Abraham's wffe Keturah. The word
Keturah means " incense "; thus the sons of Keturah are
the " incense-men," not indeed inhabitants of the far south
incense-land, but presumably the tribes whose caravans
brought the incense to Palestine and the Mediterranean
ports. So the Jlidianites appear in connexion with the
gold and incense trade from Yemen (Isa. Ix. 6), and with
the trade between Egj'pt and Syria (Gen. x.\xvii. 28, 36).
At the time of the exodus the pastures of the Midianites,
or of the branch of Midian to which Moses's father-in-law
(Jethro or Raguel, or Hobab) belonged, lay near Mount
Horeb (Exod. iii. 1); and Num. x. 29 sq. implies that the
tribe was at home in the desert of the wanderings. The
Kenites, who, in spite of their connexion with Amalek (1
Sam. XV. C), had friendly relations with Israel, and ulti-
mately coalesced with the tribe of Judali, are reiiresented
in Judg. i. 16, iv. 11 as the kin of Moses's father-in-law.
The Kenites, however, can have been but one fraction ef
Midian which took a separate course from their early
relations to Israel.' Tlie main body appear in Judg. vi. as
a powerful Bedouin confederation, invading Canaan from
the eastern desert, and ravaging the land as similar tribes
have done in all ages when Palestine lacked a strong
y^ The admixture of Midiauite elements in Judah and the other
border tribes of Uroel is conlirmcd b.v a comparison of the names of
tko ilidianile claus iu Geiu xxv, 4 with tlie Hebrew genealogies
U Chreo ii. 46, iv. 17, v. 24; Gen.-xlvi. 8).
government. VTith their defeat by Gideon and another
defeat by the Etloniites in the field of Moab, probably
about the same time (Gen. ixxvi. 35), the recorded history
of Midian closes.
A pl.ice Iilidian is mentioned 1 Kings xi. 18, nud in later timoa
the name lingered in the district east of the Gulf of 'Akaba, where
Euscbius knows a city Madinn in the country of the S.iracc-ns and
Ptolemy places ilodiana.' Still later JIadyan was n station on tlio
pilgrim route from Kgypt to Jlecca, the second beyond Aila (Elath).
Here iu the Jliddlc Ages w.is shown the well from whi.li Mo$«
watered the flocks of Sho'aib (Jcthio), and the place is still known
as "the caves of Sho-aib." It has considerable niins, which hare
been described by Kiippcll {Ficisai, 1829) and Kurton (Land of
Mkiimi, 1879).
MIDNAPUR, a district in the lieutenant-governorship
of Bengal, India, between 21° 37' and 22°- 57' N. lat., and
between 86° 35' 45" and 88° 14' E. long., is bounded on
the N. by B.-inkurd and Bardwdn, on the E. by Hooghly
and Howrah, on the S. by the Bay of Bengal, and on the
W. by Singbhiim and Mdnbhilm, with an area of 5082
square miles. Its general appearance is that of a large
open plain, of which the greater part is under cultivation.
In the northern portion the soil is poor, and there is little
wood. The country along the western boundary, known
as the Jungle Mah.'lls, is undulating <and picturesque ; it
is almost uninhabited. The eastern and south-eastern
portions are swampy and richly cultivated. The chief
rivers of the district are the Hooghly and its three tribu-
taries, the Riipn.-ir.^yan, the Haldi, and the Rasulpur.
The Midnapur high-level canal runs almost due east and
west from the town of Jlidnainir to Ulubariii on the
Hooghly 16 miles below Calcutta, and affords a continuous
navigable channel 53 miles in length. There is aUo
a tidal canal for navigation, 26 miles in length, extend-
ing from the Riipndrdyan river. The jungles in the
west of the. district yield lac, tasar silk, wax, resin, fire-
wood, charcoal, ic, and give shelter to large and small
game.
The census of 1872 rctunied the population of Jlidnapur al
2,540,963 (1,257,194 males and 1,283,769 females), including only
1-22 Europeans and 157,030 Jilohammcdans. The aboriginal tribes
belong chiefly to the jungles and hills of Chuti.i Kagjmr and Ban-
kur.i; the most nunicrons of thcni arc Snnt.ils (96,921) and Uhuniijs
(35,344). Of liigh-cnstc Hindus the returns show 136,500; and tht
number of Kayasths is given as 101,663. Among the semi-Hindu-
ized aborigines, the most numerous arc the Bagdis, a tribe of culti-
vators, fishermen, and day-labourers (76,825). Belonging to ogri-
cultural cnsti'S tliere are 1,018, 6S6. The four municipalities are
Midnai.ur (31,491), Ch.iudrakona (21,311), Chatal (15,4921. and
Tamliik (5849). Kice is the staple crop. Irrigation is ell'ected
chiefly from the high-level canal. Kent rates vary frnm lO^d. an
acre for the poorest quality of rice land to 18s. an acre for the l>c«t
irrigable lands. The district sufTcis occasionally from drought ;
AockIs are common, and very disastrous in their results. -The prin-
cipal exports are rice, silk, and sugar ; and the chief imports con-
sist of cotton cloth aud twist. Salt, indigo, silk, mats, and bnsa
and copiH-r utensils are manufactiueil. Apail from the rivers, com-
munication is alTordcd by 482 mih s of road. The total revenue in
1870-71 w-.as £$62,578, and the cx|>enditurc £53,777. The pre-
vailing diseases ait fever, diarrhrca, dysentery, and cholera. The
average mean tcniperaturc is 80° Fain., and' the average annual
rainfall C6 inches.
The tnrlv history of Slidnapur centres ronnd (he ancient town of
Tambik, which in the beginning of tlie 5th century was an ini)>oi-t-
ant Hnddhist settlement and maritime harbour. The Unit con-
ncNion of the English with the district dates from 1760, wIku Jlir
K.isim ceded to the East India Company Jlidnapur, Cliittagong,
and Bardw.in (then estimated to furnish one-thir.1 of the eiitin-
revenue of Ccngil) as the price of his elevation to lh« throne of
Beng.il on the dejiosition oI^Mir Jafar.
MiDX.vprR, chief town and headquarters station of th«
alx)ve district, is situated on the north bank of the Kasdi
river, with a population in 1872 of 31,491. The town has
a large bd:di; with commodious public offices. It is healthy,
dr)-, and well supplied with "water. An American mission
maintains an excellent training school, together with a
printing iwess, and has founded several vilhige schools in
M I D — M 1 D
285
•ihe aistrictT' Its efforts have been particularly successful
among the SantAIs, and some of the earliest and most
valuable works on their language have issued from the
Midnapur mission press. A brisk manufacture of brass
and copper utensils takes place in the town ; it is also the
centre of a large indigo and silk industry.
MIDRASH. Like all nouns of a similar lorm Afidroih
is the equivalent of the NijA'al participle,' and as such
yields as many modified meanings as the root Darosk
(15^7), to search, A-c, itself has. The practical significa-
tions, however, of Midrask, taken in historical order, are
as follows: — (1) a book of records; (2) a recension of
older, especially historical, materials ; (3) search in and
explanation of the Scriptures, notably the Pentateuch (in
which case the plural is invariably Jfidrashoth) ; (4) theory
as distinguished from practice ; ^5) a college for study
and teaching ; (G) an Agadic (that is, a free) explanation,
in contradistinction to an Jhdiikhic one ; (7) a collection
of such free explanations (in which case the plural is
Midraskim and occasionally also Midrashoth). Of these
seven significations (1) and (2) are to be found in the Bible,^
(3) and (4) are mentioned for the first time in the Misfi-
nnh,' (5) is to be met with in the Midrask,* while (6) and
(7) are to be found in early Rabbinic writings.^
The subject of this article will be — (1) the nature of
Midinsk in the sense of Agndah, to the exclusion of
llihdliah (for which see Mishxab), and (2) the develop-
ment of tliis ilidrnah Agndah into books (Midraskim).
The thinking reader of the Scriiitures cannot have failed
to observe that by the side of their ceremonial element, be
it' negative or affirmative, permissive or jussive, there is
also often to be mot with (and sometimes so as to be insepar-
able from it) a spiritual element. This spiritual element
rests chiefly on feeling or emotion, and produces pious
works only indirectly. Now the exiilanation or application
of this element, either by the Scriptures themselves or by
the rabbis, is traditionally called Midraxk Ihigc/adah
(recitation, preaching) or 3/idrnsk Agadah ' (binding the
soul to God and all that is godly).
This Iliigijitdnh or Agndnk varies considerably both in
nature and form. In its nature it sometimes humours, at
other times threatens ; it alternately promises and admon-
ishes, persuades. and rebukes, encourages and deters. In
the end it alwaj-s consoles, and throughout it instructs and
elevates. In form it is legendary, historical, exegetic,
didactic, theosophic, epigrammatic ; but throughout it is
ethical.
And varied as was and is the Midrnxh Agndak, so varied
have been its fortunes. \Vhilst at times it stood very
high in the estimation both of the teachers and the con-
gregatioP3 in Israel,' it sank at other times very low
indeed." iv'ay, at one and the same time, whilst some
' Conip. Xeheni. viii. 8, where NTpD3 evi.lently stands fer ^<^p^n.
See nl.io Kinilii on 2 Cliron. xiii. 22. and Schiller-Bzinessy, E:ciJOsUloii.
&c., C.-imi)rii1gc 1882, p. 11. ' 2 CDiuo. liii. 22 and xiiv. 27.
' See Sclnrim, iv. 3, unci Jboth, i. 17
* Dcrohlth nabhih, c. Ixiii. (on Gen. xxv. 22): n:^'!^ K^ N^HI
, • • -\ySi\ Dt;'> ^C lE'^^Db N^N- ^Ii<lra$h is nse<l in the East to this
day lor Drth Jlammidrash. See MS. Oo. 6, 63 (of the University
Libr.iry, O.imbri.lgc), leaf 135a, lower margin (itJ'TTD^ ^-[p DDI
■•• Debts').
' Raslii (f.j., on Gen. iii. 8) nnd Tosophalh, passim.
' Tliose who identify this word as merely the Chaldaic fonn of the
Hebrew Ilafja/aflth (and they have, certainly, some authority on their
Hide) ought to write It Aggadnh [n']^^'i, which, however, is not the
traditional spelling of it (iTJJSl. Singularly enough, the Latin religio
is similarly derived by some from rrllfjare and by others from rfliijrre.
' Siphcrt on Deut. § 49 : " If thou wishest to know Him who but
spak* and the world came into being, leam llogr,adah ; for by so doing
thou wilt recognize the Holy One (blessed be He I) and cling io Hii
Trays ! "'
•T. Y., itastroth, Ui. 4: " Ami R. Ze'erah was teasing those rabbis
cf the Agadah."
rabbis exalted it to the skies,' other rabbis treated it?
with hatred,'" or, worse still, with contempt." There have
actually been teachers whose treatment. o£ iC Jifferea with
the difierence of the occasion.'' The fact is the Jews
liked or disliked the Midraeh Agadah according to their
political condition on the one hand and their proximity
to Jewish professors of Christianity on the other. In the
hour of prosperity the Jews preferred the Hatahkak ; "
in that of adversity they ran to hear the consoling words
of the Agadah.^* When near Judseo-Christians, wbosa
religious strength and argimient chiefly rested on Agadah,^
the Jews disliked it ; when among themselves, or when
dwelling among Gentiles (heathen or Christian), they
showed their wonted partiality for it.
But, whatever were the likings or dislikings of the Jew*
for the Midrashot/i, it is certain that these traditions were
early '" committed to writing, and formed into sjjecial
volumes, known as " Books of Agadah." " Such were first
some of the Targunwn and then the Midrashiin. Against
writing down the traditional exijlanations of the Jlosaic
ceremonial there existed a distinct law," which was observed
down to near the end of the 6th century. At an earlier
period isolated disciples only, in order to refresh their
memory, wrote down short Halakhic notes, which, how-
ever, they kept in secret." The Tavguviim and Midrashiin,
on the other hand, were composed very early and were
numerous, while their extensive contents were circulated
in public.
The Midrash, from whatever point of view it may be
regarded, is of the highest value. It is of the highest
value, of course, to the Jew as Jew first, inasmuch as ha
finds there recorded the noblest ideas, sayings, and teach-
ings of his venerable sages of early times. In the next
place it has value to the Christian as Christian, since only
by these ideas, teachings, reasonings, and descriptions can
the beautiful sayings of the Founder of Christianity, th«
reasonings of the apoitles, and the imagery of the sublime
but enigmatic Apocalypse be rightly understood. But its
importance appeals albo to the general scholar, because of
the inexhaustible mines of information of all kinds it con-
tains. The philologist will find here numerous hints on lexi-
cography and grammar, chiefly, of course, of the Semitic
languages, but also of other tongues, notably Greek ar.d
Latin. The historian will gather here a rich harvest oa
geography, chorography, topography, chronology, numis-
matics, itc. The philosopher will find here abimdant and
' foid.: "Then s.aid to him R. Bo b.ir [.son of] Kohano, Why dost
thou tease them ? Ask, and they will surely answer thee ! "
"T. Y., Slwbbalh, x\± 1: " He who holds it forth becomes burned
by it ; he who listens to it gets no reward."
" Ibid.: *' I never in my life looked into Agadic books."
'^ Ibid.: "Let the hand of him who wrote it bo cutoff"; and com-
pare with this T. B,, Jioho Diilhro, 1236: "goodly pearl."
"Beginning of Pesil'dho J3nhoi'esh J/asshdislii : " First when the
money was at hand one de.Mred to hear the woixl of the iliahnah and
the word of the Talmud. . . ."
^* Ibid.: " Xow, however, when the money is not to be got, and,
moreover, when we are sick in consequence of the (treatment by the)
government, one pines for the word of the Bible and for the woi-d of
the Agadah.'^
" T. Y., Khahhnth, xvi, 1, and T. B., Shaliaih, 116a : "The Evan-
gelia and other Christian writings."
** See Tosephto Shabbath, xiv. : " I remember that one brought before
Rabbai Gamliel the elder [St Paul's teacher] the book of Job (in the)
Chaldaic paraphrase"; and T. Y., Kilayim, ix. i: "At that time I
ran (my) eyes through the whole Book of the Psalms (in the form) of,
the Ilnggadah [Agadah of the Psalms]," K. Biyya Rubboh belonged
to the middle of the 2d Christian century.
'" NmJST »1ED- See T. B., BeraUwCh. 23a. Temurah, Ub, and
the Tatmndi7n, pajisim.
" T. B. , Giain, 606 : " j n the college of R. Yishm'ael it was taught.
These [see Exod. x.xxiv. 27] thou oughtest to write do^vn, bnt thou
must not write down Ifalakhoth.' "
" T.B.. Shalbath, 66: " I found a 'seci-et roll,"' that i«, a roU of
Halakhoth kept secret. Comp. Bashi. t» loco.
286
M I D R A S H
valuable notices on logic, psychology, metaphysics, theo-
logy, theosophy, aesthetics, rhetoric, poetry, mathematics,
geometry, astronomy, zoology, botany, biology, morphology,
chemistry, medicine, physics, &c. The statesman — parti-
cnlarly if he be inclined to follow the Psalmist's advice —
"from the ancients I gather understanding " (cxix. 100) —
will find here valuable information on ancient ethnography
in the full sense of the term — politics, political economy,
law, military science, naval affairs, ic. The true scholar
will find out by the study of the Agadak that many a dis-
covery thought to belong to a recent age was well known
to these ancient doctors.
The sources of the Agadah are five : — (1) the Targumim
and especially those on the Prophets and Hagiographa ;
(2) the non-canonical Mishnah (Mathnitlio Boraitho ; see
Mishnah), which contains many valuable pieces, the age
of which is often anterior, in essence if not in form, not
only to those contained in the canonical Mishnah, but
also to the sayings of the New Testament ; (3) the canonical
(officially recognized) Mishnah, which contains several
entire treatises of an Agadic nature, as Abolh,^ Middolh,
&c.,^ and numerous pieces scattered here and there among
the Halakhah; (4) both Talmtidim^ (the Palestinian and
Babylonian), which have thousands of Agadic notices
interspersed in their Halakhoth ; and (5) the Midrashim,
Kar cfox';!'. It is of the last alone, as represented by their
principal collections, that we give an historical enumeration
here : —
(1) MccjUUilh Ta'anith is an historical Midrash consisting of
twelve Pcrakim, and is called so on tlie principle of btats a no)»
liieendo, seeing that in it are enumerated tlie days of the year on
which a Jew must not fast. The Aramaic part of it alone cousti-
tutps the real Megillah, and belongs to the beginning of the 2d
Christian century.' The cditio princcps came out at llantua, 1613,
4to ; but cheap editions have been printed at Warsaw and elsewhere.
' (2) Scpli£r ye:irah is a philosophico-cabbalistic Midrash divided
into six Peralam, which, in their turn, are siibdivided into
Muhniyyoth. It is variously ascribed to the patriarch Abraham
and to R. 'Akibah, the illustrious teacher, who suffered martyrdom
under Hadrian. To this rabbi the book, no doubt, belongs both in
substance and form.^ It has gone through numerous ediuons, the
ed. print, being of 1562 (Mautu.i, 4to), and has been translated into
Latin, German, and English (New York, 3877).
(3) Othiyyoth de-Rabbi 'Akibah is a jimji-cabbalistic Midrash on
the alphabet, belonging, in essence if not in form, to the aforesaid
teacher and martyr. £d. princ, Constantinople, 1520, 4to.
(4) Massckhtth Eckhahth is an ostronomico-cabbnlistic Midrash
in seven Pcrakim. It is ascribed to I!. Yislima'el the high priest
A > A valuable edition of this trcatjse (in Hebrew and English) has
been published by Dr C. Taylor, Cambridge, 1878.
' - To these we may add, for the sake of convenience, ajthough they
do not, strictly speaking, belong to the canonical Mishnah, the Pere^
Rabbi Meir and the Agadic. parts of the Massekhtoth Ketannoth.
^ ' Two collections of Talmudic Ayadoth were made early in the 16th
century:— (I) Haggadoth Hallalmud, Constantinople, 1611, folio, of
which apparently only five copies are in existence, the finest of these
being preserved in the University Library of Cambridge ; and (2) 'En
Ya'akob {or' En Yisrad), of which numerous and cheap editions exist,
the ed. princ. being that of Salonika, 1516-22.
■ • Almost all that the latest critics have said concerning the age of
the various Sargumim and Midrashim will have to be unsaid. Not
only are negative statements difficult of proof ; in this case they are
ibsolutely incoiTect. We shall only give two cxanjplcs. The state-
ment " Vayyikra liabbah cannot be early, as Rashi did not know of it,
since ho nowhere mentions it," is doubly incon-ect : Rashi does quote
it {e.g., on Haggai i. 1). Ag:iin the statement "We must not omit to
observe that no early Jewish commentator — Rashi, Ibn Ezra, &c. —
mentions the Targum either to Proverbs or to Job and Psalms; Nathan
nen Jechiel (12th century) is the first who quotes it," contains a re-
duetto ad absurdum in itself. For Nathan b. Yehicl was, as i.i well
known, a somewhat older conlemjtorary of Rashi {ob. 1105), and lived
full a hundred years before Ibn 'Ezra!
'SeeT. B., SyiiA«iWn, 65S and 07*. In the former place it distinctly
speaks of the Sepher Yezirah (HTV IDD), and, although in the
latter place it speaks of the Ililekholh Yejirah (m'X' ni3?n), there
cannot be ■» doubt that Sepher (1BD) and UiUkhoth (ni37n) are
there identical. , Moreover, Mishniyyth and llalakhoth are, in a cer.
tarn sense, convertible terms (see JIisaniB) ; and our book (as
remarked abc-e) consltts of itii'.nii'yc(h.
Judging from interpal evidence on the one hand, and from what is
known of K. Yishma'el in the Talmudim and Midrashim {Baili
Berakh'Ah, 7a and elsewhere) on the other hand, there seems to be
no valid reason for doubting that he is the author of this small but
sublime book. This Midrash is printed in the collection Are^
Lebanon (Venice, 1601, 4to) under the title of '* Pireke Hekhahth"
and '^ MasscVuth Hckhaloth," and a MS. of it is preserved in the
University Library of Cambridge (Dd. 10. 11. 7. 2). The work,
however, called " The Greater and iLe Lesser Hckhaloih," in thirty
Perakim, printed in this century, somewhere in Poland, cont^iins,
besides the ancient literature, a good deal of matter which is of
much later date. "" ^ -- — ' ~
(6) Seder 'Olam (the Greater and the Lesser) arc two historical
Midrashim, the former of which belongs to the 2d century, whilst
the latter (which is a mere extract of the former) belongs to a laUi
ago indeed (the Goonaic). They have been repeatedly printed.
always together, the ed. princ. being Mantua, 1513, 4to.
(6) Haggadah shcl Pesah is a litui'gical Midrash of the middle of
the 2d century, as far as its main portions go. It exists now in
three principal and several minor recensions in accordance with th^
various rituals (see IIahzok), and is recited at the domestic servi'-e
of the first two Passover evenings. The editions are too numerous
to be mentioned, the ui. princ. being Constantinople, 1505, fc'.io.
(7) MetjiUath Anlioklios treats ostensibly, as its name ind-cates,
of the suiferings of the Jews under Antiochus Epiphancs, n^A their
deliverance from his tyranny, but in reality of their sufferirgsander
Hadrian and their deliverance under Antoninus Pius. Tb^ Aramaic
text, with the exception of a few interpolations, belongs to che middle
ofthe 2d century. This little "roll" was for the first time published
by Filipowsky (London, 1851, 32mo). A MS. copy of the Hebrei»
is iireserved in the University Library of Cambridge (T'd. 8. 84)
(8) Zohar {Midrash Hazzohar, Midrasho shcl Rabbi Shimeon b.
Yohai, Midrash Yehi Or, ic. ) is a cabbalistic Midrash on the Peii-
tateuch. Canticles, Ruth, and part of Lamentations. It is variously
ascribed to the famous R. Shim' eon (disciple of R. 'Akibah, 4c ) and
to R. Mosheli b. Shemtob of Leon (a second-rate cabbalist of the
time of Nahmanides and Ibn Addereth). The Zoluir belongs,
strictly speaking, to neither of these, whilst, in a certain sense,
it belongs to both. The fact is — the nucleus of the book ia of
Mishnic times, and R. Shim'eon b. Yohai was the author of the
Zoliar in the same .sense that R Yoliatian was the author of tbt
Palestinian Talmud, i.e., he gave the first impulse to the comiwsi-
tion of the book. But R. Mosheh of Leon,' on the other hand, was
the firet not only to copy and disseminate the Zohar in Europt,
but also to disfigure it by sundiy explanatory interpolations. For
more details see Lumby, "Introduction to the Epistle of Jude," in
the Speaker's Commentary, vol. iv. p. 388. The first two nlitioDS
of the Zohar ' on the Peutateuch came out simultaneously (^lanttia,
1.158-60, 4to, and Cremona, 1558, folio), and the ed. princ en
Canticles, Ruth, and part of Lamentations came out at Saloniki
(1597, 4to) The best, though bv no means critical, edition on the
Pentateuch is that of Brody, 181^3, Svo. Of translations, such tt
they are, there exist those of Knorrv. Rosenroth, Kabbala dcjitidalm
(vol. l,Suizbach, 1677, and vol. ii., Frankfort, 1684, 4to), and
Tholuck, Wichligc Stellen, kc. (Berlin, 1824, Svo), ic.»
(9) Pesikotho' (commonly, but by mistake, called Pesilda)
dcrab Kohano is a homiletic Midrash consisting of thirty-two
Pcsiktolh for the principal festivals and fasts, and the historically
noted sabbaths and other days. It is of the end of the 3d or the
beginning of the 4th century. Having been but rarely quoted
since the 12th century, so that most scholars knew of it only
• R. Mosheh of Leon is a fair sample of the mediocrity of his time
in cabbalistic lore, aud combined, as is usual, with his nkediocrity an
ill imiUble vanity; see MS. Dd. 11. 22 (Cambridge University Librarj),
leaf 2a: " And 1 adjure every one who should deeply study this book,
or who should copy it, or read it, that he do not blot out my name
from my property (inheritance), for I have comiwsed it. . . ," Tliit
statement alone would suffice to prove that R. Mosheh of Leon could
never have ascribed a book composed by himself to anybody else.
' The Zohar, cleared of the main works by which it is surrounded,
and of the interpolations by which it has been disfigured both by its
first European copyist and by others down even to our own days, wa»
begun in Palestine late in the 2d or early in the 3d century, and
finished, at the latest, in the 6th or 7th century. It is impossible
that it should have been composed after that time and before the
Rcu.iissancc, as both language and contents clearly show.
• Whilst the principal editions of the many textual extracts'made
from the Zo/iar (as the Iddctoth, &e. ) need not be specilied here, those
of the following supplementary and kindre'd works ought to bo men-
tionedi— (1) Tikkmie llii:z:Jiar {ed. princ. Mantua, 1557, 4to), and
(2) Zohar Iladaah {ed. princ. Cracow, 1603). Nor should the Kontra
mijseplier }/azxhar, Hibburo Tinyono (by the otherwise very Icuned
Yitshak b. Mo^hch of Sntauow) b« passed over. It it a mere imitatio^
of the Zt'har, — an imposition of a kind which it a disgrace to literature.
• For the three Midmihin—itekhiUo, Siphro, and Siphtre—*el
under MisaNan.
M I D R A S H
287
indirectly, it was long considered lost, till, in 1868, Salomon Bnber
of Lemberg, a man of learning, wealth, and love for the ancient
literature of his nation, edited it from four M3S., one of which
(formerly in possession of Carmoly) is now preserved in the Uni-
Tersity Librnry of Cambridge (Add. 1497). The printed edition
appeared at Lyck, 8vo.
(10) I'esiklo Rabhathi, consisting in the latest edition of eighty-
four Piskoth, is a Midrash of the same nature, and, in its main part,
almost of the same date, as (9). Both drew from the same sources.
This Midrash has been edited five times, — the latest, best, and
cheapest edition being that of Friedmann (Vienna, 1880, 8vo).
(11) Tanna debe Eliyijahu consists of two parts, the Greater
(Rabbo) aud the Lesser (Zutto), — the former in thirty-one and the
latter in twenty-five Pc'dkim. It is an exegetical Midrash, the
name of which is alreaily known to the Bcrtshith Rabbah (c. liv.)
and the Babylonian Talmud {Kelhuboth, 106a). It ia only un-
critical criticism that can declare it a Gaonaic work, although, like
all other old books of the Jews, it is not without later additions.
£d. princ.^ Venice, 1598, 4to. There are modem and cheap Polish
editions.
(12) Midrash Jiabbah (nil) or Rabboth (nm) is chiefly an
exegetical and homiletical Midrash on the Pentateuch and the
"Five Rolls" {Hamcsh Megilloth, i.e.. Canticles, Ruth, Lamenta-
tions, Ecclesiastes, and Esther). It is called Jiabbah either from
the third (the first distinctive) word of its beginning (''VtS'lD '2T
- . . n31) or from its being the most voluminous* Midrash ; hence
also Rabbo (N31). The Midrash on Canticles (and Ecclesiastes)
is now and then also c^Wed Midrash Ifazithn (from the first distinc-
tive word of the beginning n^TH). These ten Midrashim are,
certainly, of various styles and ages ; yet none of them is, inter-
polation excepted, later than the beginning of the 5th century.^ It
IS remarkable that, although th&Mcgilloth themselves had been early
attached to the Pentateuch (since they .were long before the 10th
century, and still are, read through the synagogaf year, even as was
and still is the Pentateuch itselO, the Rabboth had no common
tditio princcps^ — that on the Pentateuch appearing for the first time
' The Rabbah on Genesis has 100 Parshiyyoth, that on Exodus 52,
that on Leviticus 37, that on Numbers 23, and that on Deuteronomy
11. These five Midrashim are quoted according to their chapters. The
Ral^h on Canticles acconmiodates itself to the sacred te.\t, and is
quoted accordingly. Ruth has 8 Parshiyyoth, aud is quoted according
to these. Lamentations has 1 chapter consisting of 33 introductions
{Pcthihotho Dehakkime), accommodating itself, for the rest, to the
sacred text. Ecclesiastes has 3 Sedarim, and Esther has 6 Parshiyyoth.
At various times various mod-^s of quoting these Midrashim are
current, — the most common and most expedient, however, being that
of quoting them acconling to the verses of the Bible.
* Here might with advantage be mentioned some pieces of literature
which are kindred in nature, although some of them are of much
earlier date, whilst others are much later, than the ten Midrashivi
just mentioned: — (1) Aynduth Bereshilh on Genesis, in eighty-three
chapters, — edited for the first time by R. Menahem de Lonsauo in his
f>hcte Yadoth, Venice, 1618, 4to; (2) Midrash Vayyisan on Genesis
XXXV. 5, in one chapter, — to be found in Jellinek's Let hii-Midrasch,
Leipsic, 1855, Svo ; (3) amplifications of chapter Ixx. of our Midrash
Rabbah, on Genesis iiviii. 22, by the incorporation of the whole
Apocryphon Tobit in Aramaic, &c. (see The Look of Tobit, kc,
Oxford, 1878, Svo) ; (4) Midra.'h Viiyyosha on Exodus xlv. 30, xv.
1-18,— printed at Constantinople, 1519, 4to ; a MS. of this Midrash
IS preserved in the University Library, Cambridge (Add. 85-1) ; (5)
Hidrash 'Ascrcth Haddibbcrolh on Exodus xx., — printed in Jellinek's
bet ha-Midrasch, Leipsic, 1853, Svo ; (6) Midrash Pelirath Aharon
on Numbers ix. 23-29 ; (7) Midrash Peti.nlh Moshch on Deuteronomy
xxxiv. ; (8) Midrash Abbo Gorion on Esther ; the last three are to be
found in the before-meutioned Bel ha-Midrasch ; (9) Midrash Shemnd,
also called, from its beginning, 'Eth la'asolh Ladouai, Constantinople,
1517, folio; (10) Midrash Voiiah, Prague, 1595, 4to; (11) Midrash
Tdlim (Tehiltim), 1512; (12) .Midrash Mishele, 1517; the last two
are printed at Constantinople, and in folio ; (13) Srpher Ilayyashar
(in which a good many old traditions are preserved, although it is,
of course, not the one mentioned in various books of the BiWe),
Venice, 1625, 4to ; (14) Dibtre Jlayyaniim shel Mosheh, (ijnstanti-
nople, 1516, 4to ; a fragment of this is to be found in MS. Add.
632. 4 in the University Library of Cambridge ; (15) Vosephon (or
Josippon), various works of Flavins Josephus worked up rather freely,
Mantua, 1480, folio,— translated into Latin (German and Spanisli)
•everal times ; (161 Zerubbabel, Constantinople, 1519, Svo ; (17) Elleh
Ezkerah on the " Ten Martyrs. " For several other smaller Midrashim
tee Jellinek's Bet haMiJrascIt, i. and ii,, 185-3, iii., 1855, iv., 1857,
all at Leipsic ; v., 1873, and vi,, 1877, both at Vienna ; and comp.
■Uo Horowitz, Sammlung Klrinrr Midraschim, i., ii., Frankfort,
1881-82. The Midrashim on Isaiah and on Job seem now irretriev-
ably lost
• A« if to compensate for this drawback, the well-known Comelio
Adelkind brought out at Venice, in 1545, two editions of the RabboUt
«u tke Pentateuch and MeQUloth, the one at Bombergi's house aud the
in 1512 (Constantinople, folio), and that on the ilegilloth in 1619
(somewhere in Italy, flN'^ti'K Hinoa. also in folio).' The latest
and best edition is that of Vilna, 1880, folio. A translation in
German is now coming out at Leipsic, by Dr A. V7iin3che.
(13) Pircke de-Rabbi Eh'ezer (also called Boraitlw dt-Rahhi
Eliczcr) is an astronomico-theosophical Midrash consisting of
fifty-four Perakim. It goes through the so-called "eighteen bene-
dictions," the signs of the zodiac, ic, but is unfinished. It belongs,
no doubt, to the 5th century. The fact that the name " Faiima **
occui-s in it is no proof whatever that the look is post-JIohammedan,
as that name must have been already known to the idolatrous Arabs.
Ed. prin., Constantinople, 1514, and with a Latin translation,
Leyden, 1644, both editions being in 4to, There are also now
to be found cheap editions (Lemberg, Warsaw).
(14) Tanhuma is an exegetical and homiletical Midrash on the
whole Pentateuch. It is quoted accoviing to the Parshiyyoth of
the week. Although originally of the end of the 5th or the
beginning of the 6th century, it has now two priucipal additions,
which form part of the book ; — (1) several of tlie Shcethth of Eab
Aliai Gaon (of the 8th century), and (2) several pieces of the
Ycsodoi R. Mosheh Haddarshun, of Narbonne(of the 11th century).
On its relation to the ''Yelavimrdenu^' (often quoted in the lltb
Century, but supposed to be lost) light will soon be thrown by the
before-mentioned Salomon Buber, who is now preparing a critical
edition of it. The ed. princ. of the Tanhuma is Constantinople,
1522, folio; and a very valuable ilS. copy of it is in the Cam-
bridge University Library (Add. 1212).
(15) Bahir is a small cabbalistic Midrash ascribed to the pre-
ilishnic teacher, R. Nehunyah b. Hakkanah, — no doubt from
its beginning with the words.- •• njpn'p n<:im '3T "IDX-
Nahmanides {ob. c. 1268) quotes this book often in his commentary
on the Pentateuch, under the names of Sepher Babbahir, or of
Midrasho slicl Rabbi Kchunyah b. Hakkanah. Some have pro-
nounced this work a iate fabrication, but others, who have
thoroughly studied it, justly describe it as "old in substance if
not inform." frf.^n'nc, Amsterdam, 1651, 4to. A cheap edition
appeared at Lemberg (1865, Svo), and a SIS. of this work is pre-
served in the University Library of Cambridge (Dd. 10. 11. 4).
(16) Yalkiit is the only existing systematic if not exhaustive
collection of the Agadoth on the whole Bible. Its author drew not
only from most of the Midrashim named in this article, but also
from the Boraithoth (see JIisu>'.vH), both Talmtidim, and the
Midrashic works now lost (as the Jbkhir, Easshckhcm, or
Hashkem, &c.).' This fact constitutes one of the principal points
of its value. The author was R. Shim'eou, brother (and not sou)
of R. Helbo, and father of the distinguished grammarian, critic, and
divine R. Yoseph Kara. He lived somewhere in the north of France
in tlie 11th century. The ed. princ. of the Yaihit on Ezra,
Xehcmiah, and the books of Chronicles came out at Venice, 1517,
folio (in the first Rabbinic Bible) ; that on the Prophets and
Hagiographa in 1521, and that on the Pentateuch in 1526-27, both
at Salonika, and in folio. An English translation of the whole
work has been undertaken by a band of Rabbinic scholars in
Cambridge. The first instalment, "The Yalkut on Zechariah,"
by E. G. King, B.D., Hebrew lecturer of Sidney Sussex College,
appeared in 1882. This specimen, besides giving a correct trans-
lation, contains many valuable notes.
(17) Lckiih Tob is a Midrash on the Pentateuch and the five
MegiUoth.'hy R. Tobiyyahu b. Eli'ezer of Greece, who lived during
the crusade of 1096. 'This work draws, certainly, upon the old and
well-known Midrashim, and as such it would have thoroughly
tleserved the censure passed upon it by the witty but somewhat
irreverent Abraham Ibn Ezra (in his preface to his commentary
on the Pentateuch). But the Lekah Tab h.as also most valuable
exjtlanations both by the collector himself and by his father (R.
Eli'ezer), a fact passed over by Ibn 'Ezra in silence. The Lckah
Tob on Leviticus. Numbers, and Deuteronomy canie out for
the first time at Venice, in 1546. folio, under the title of Pcsikto
Ziillarlo (see leaf 934 in the postscript by the editor, Nnp'DDn
NmUlt, which explains the somewhat vagtie title on the title-
p.igo Nnai IS Nmun Snp'DD). in 1753-54 it was repub-
lished at Venice, with a Latin translation, by Blasius Ugolinus
iu his Thesaurus Jntiquitalum Sacrarum (xv.-xvi. ) under the
name of PesicHui. Tlie Lrkah Tob on Genesis and Exodus was
other at Giustiniani's. These two editions differ in nothing but in
the title. page.s. ic, and the vignettes of the various books. The
former edition is in possession of Dr W. Aldis Wright, an.l the latter
in that of Dr C. Taylor. The fact of these editions having appeared
simultaneously is, apparently, unknown to the bibliographers.
• It is noteworthy that in this edition Ahashterosh, i.e., Esther,
stands between Lamentations and Ecclesiastes, with which latter tht
Midrash on the Megilloth ends.
' We may mention here the ed. princ. of three cabbalistic-Midraahic
colleitions which go under the name of Yalkut :— (1) Yalkvt Hadeuk,
Lublin, 1648, 4to ; (2) Yalk,U Reubeni Hakkutnn, Prague, I6M.
4to; and (3) YalkiU Reubeni UaggadoL Wilhcrmsdorf, 1681, folio.
288
M I E — M IE
5^ublislied, with a mtioal commentftry* at Vilna, by Salomon Bnber
1880, 8vo), where also simultaneously a third edition of this
.ilidrnsh on tlio last three books of Moses, with a short commentary
on it, came out by Aharon filosheh Padova, of Carlin. Tht Lckah
7'ob on the five Mcgilloth is as yet unpublished ; there exist, how-
ever, several good MSS. of it, both in public and private libraries,
the finest copy in every respect being that preserved in the Uni-
versity Library, Cambridge (Add. 378. 1).
(18) Mciwrath Hammaor ia a scient:5c, though incomplete,
ooUc'Ction of the principal Agadoth of the Talmudim and
JJ/;rf?-a5Azm,byR. Yizhak Abohabtho elder( flourished 13th century).
The editions, with and without translations, are very numerous, —
the cd. princ. being Constantinople, lol'i, folio. There are trans-
lations in Spanish, Jud?eo-Gcrman, and German, but not in English.
Wo append two specimens of Midrashun^^-the first from
PcsikothOj leaf 1276, and the second from Midra^h Slicvwth JtabbcUt,
cap. ii.
First Specimev.— The Holy One (blessed be He!) said to the Prophet^,' Go ye
and comfort ye Jerusnlcin I
Then went Hosea lo comfort her and sold. The Holy One (blessed be He!) wnt
me to tliee lo comfort ihee. She said, Wliat bust tJiou in Ihlnc band to comfort
me? The Prophet said (xiv. 6 [5]), " 1 will be as the dew unto Israel: " But
Jerusdlem said to him, Only yesterday thou tuldcst me (Ix. !«), " Epiiralm Is
Bmltltn, their root is dried up, they shall bear no fruit: yva, though (hey bring
forth, yet will I slay even tlie beloved fiiUt of , their womb!" ond now thou
speukcst to me thus. Wlilch shall we believe, the first or the second prophecy ?
Then went Joel to comfort her and said. Tho Holy One (blessed be He!) acnt
me to ihce to comfort thee. She said to him. What hast tliou in thine hand to
comfort mc? The Piophet said (iv. 18). "And it shall como to pass in that
day that the mounUiins shall drop doM-n new wine, nnd the hills shall flow with
milk. J:c.! " But Jerusalem said to him. Only yesterday thou toldest me (1. 5),
" Awake, ye drunkards, and weep; and howl, all ye drinkers of wine, because of
the new wine; for It la cut off from yoiir moulh! " and now thou speakest to me
thus. Which shall we believe, the flist or the second pmphecy?
Then went Amos to comfort her and said. The Holy One (blessed be He !) sent
mc to thee to comfort thee. Slic said to him, What hast thou In thine hani to
comfort me? Tho Prophet said (ix. 11). " In tliat day will I raise up the taber-
nacle of David that Is fallen I " But Jeinisakm said to him. Only yesterday thou
toldest mc (v. 2), "The Virgin of Israel is f.illen; she shall no more rise!" and
now ihou speakest to me thus. Which shall we believe, the first or the second
prophecy?
Then went Micah 2 to comfort her and said. The Holy One fblessed be He!)
sent me to thee to comfort thee. She said to him, What hast thou in thine lund
to comfort me? The Pif^phct srid (vil. IS), -'Who Is a God like unto Thee, that
pardoneth iniquity and passeth by the transgression of the remnant of His
heritage?" But Jerusalem said to him, Only yesterdny thou toldest nic (1. 6),
" For the transgression of Jacob is all this, and tor the sins of the house of Israel,
Ac!" and now thou spc.ikest lo me thus. Which shall we believe, the first or
tl*e second prophecy?
Then went Nahi;m to comfort her and snid, Tlie Holy One (blessed be He!)
sent me to thee to comfort thee. She said to him. What hast thou in thine hand
to comfort me? The Prophet said (d. 1 (i. 15]), - For the wicked shall no more
pass through tliee!" But Jerusalem said to him. Only yesterday tliou toldest
me (i. 11), " There is one come out of thee thm imagincth evil apiinst the Lord,
0 wick?d counsellor!" and now thou speakest to me thus. Which shall we
believe, the first or the second prophecy.?
Then went Hadakruk lo comfort her and said. The Holy One (blessed be He!)
ficnt me to thee to comfort thee. She snid to him. What h.i^t thon in thine hand
to comfort me? The Prophet said (iii. 13). ■* Thou ucntcst forih for the sulvation
of Thy people, even for the salvation with Thine Anointed One ! " But Jerusalem
Eiiid to him. Only yesterday thou toldest me (i. 2), " 0 Lord, how long shall 1 cry
and Thou wilt not hear, even C17 out unto Thee of violence and 1 hou wilt not
save!"' and now thou speakest to me thus. Which shall we believe, the first or
the second prophecy?
Then went ZEniANiAn to comfort her and said. The Holy One (blessed be He!)
sent me to thee ro comfort thee. She said to liim. What hiist thou in thine hand
lo comfort roe? The Propliet said (i. 12). " And it ^hall come to p^i-s at that time
that I ahall scorch Jerusalem with lights!" But Jerusalem said to him. Only
ycsturday ihi-u toldest mc (i. 15). "A djy of darkness and glormincss! " and now
thou speakest to me thus. Which shall we believe, the first or the second
proi)liccy?
Then went Hacoai to comfort her nnd said, Tlie Holy One (blessed bo He!)
sent pic to thee to comfort ihee. She said to him, What hast ihou In thine hand
to comfort roe ? TJie Prophet said (il. 19), " Is tho seed yet in the barn ! Yea. as
ytt the vino and tlie fig tree and the pomcgianate and the olive ti-ee hath not
brouglit forth: from this day will 1 bless you!" But Jerusalem said to Iilm,
Only yesterday thou toldest roe (I. C). " Ye have
&c.r'nnd now thou speakest
the second prophecy.
Then weht Zkciiatiiaii to comfort her and said. The Holy One (blessed be He!)
sent roc to thee to rororort thee. She said to hlro. What hast iliuu in thine hand
to comfort mc? The Prophet said (I. 15), -And I om very sore displeased Miih
the heathen tliat nve at ease ; for I was but a little displeased nnd they helped
forward the offliction I " But Jcruaulem said to him. Only yesterday Ihou lolilest
mc (I. 2), "The Loid hath been sore displeased with your faihc * " "" ^' " "
BpeaLc '
Then we
. Ma
Tifoit Ihee. Slie said to him. What hast thou in thine hand
10 comfort roe? The Prophet said (lli. 12), "And all natu-n* shall call you
blessed • for yc shrill be a dcllRhtsome land I " But Jvi-usalcm said lo him. Only
yctcrday thou toldest roe (i. 10), "I have no delight In you!" nnd now thou
epi-nkest 10 me thus. Wlilch ahull we bcliove, the fiist or the last i-rophccy?
Then went nil the Prophets to tho Holy One (btesAOil be He!) haying to Him.
Lord of the Untveisc. Jcruaulem will not accept con-ohilion at ..ur hands. Then
the Holy One (blessed bo He!) sntd to them, *' I and you *lll together go to
tomfort her; and this is why It soys (Isaiah xl. 1). Cmfort 3 c, comfort yc m
l-EOpLE comfort her wmt mi.,3 Comfi.rt her, ye cele-tml ones! comfort her, yo
tcrrvstvial ones! Comfort her. yo llOng ones! comfort h^r, yo dead ones!
Comfort her In this world 1 comfort her in the world Income '.
' > Comp. Pfikio Ii'ibbnf?ii, cd. Frledmnnn, loaf 13<!ft.
» Sue Pesiiro Rubba'hi (cd. Filcdmann, leaf 1386), wh.-tv U snys (before the
parngraidi on Nahum), •' 'Obudyah prophesied for Edom, nnd Yooiih fur -Mncveh."
This, It Is true, Is a mcrt glosa; but It b tho irue reason wliy ihoc two propheM
a There U n play here upon tho mcnnlnp of the Hebrew. »oy, which way be
itt&^l either 'Ammt{'*wy people") or 7mmi {" with mc").
SucoTn* SpEcimR.— And whom doett He tryf Ths rtRhteooa one; for H mm
(Pa. xl. &). "The Lord tricth th« rightAOOH." And by wliftt does He try him? B^
the feeding of sheep. David He tried by thcep and found hint • good shepherd;
for It Bays (Ps. IxxvlU. 70), ** And H« took him from tho ' rc»tndnu ' of sbe<rp."
What is the meaning of 'Mimmikhleothf The root Is the same as that of 'm^^^-
kale [^^agyelh^m) (Gen. vili. 2), "And the rain wa» restrained." David restrabied
the btg sheep In favour of tlie sroatl onrs. lie brought out first the young ones,
so that they should feed on tho tender herbs; then he brought out the old oaes
that they should feed on the less tcndet' herbs; and, tlruklly, be biought out tha
strong sheep that they should feed on Uic coarser herbs. Upon thi* the Holy Ono
(blessed be He!) said, He who undcrstandetb lo feed sheep according to their
strength, let him come and feed kly pcoplcl And this it is xthat is wiltten
(Pa. Ixxvld. 71), " From following the ewes gicat wiUi >oung He bieught him to
fi^d Jacob His people!" And Llie same was the case as regards Uoses, whom
the Holy One (blessed be He !) tried by sheep. Our j abbls say, When Woica our
teacher (peace be upon hirol) was feeding the sheep of Jethro In the wlldeines^
a kid ran B>\ay from hiro, and Uoses ran after it till they came to a mountain,
hollow. When it had reached the mountain-hollow tliere was ■ pool of water,
and the kid stood still in ordi-r to dilnk. When Uoses 1 cached the kid he said to
it, I did not know that thou didst run away from roe because thou wast tlrfrsty and
faint. Thereupon he put It on his shoulJeis and walked back with It lo tha
flock.* Tlicn said the Holy One (blessed be He!), Thou art compassionate in the
feeding of sheep belonging to mere flesh and blood (man); as thou Dvest, ihoa
Shalt feed My flock, even Israeli Behold, Ihls it ta that Is wiilten (Exod. 111. 1),
" And Hoses was feeding the flock, Ac." (S. M. S.-S.)
MIEDZYKZECZ PODLASKI (Russian, Mejiryechie), a
district town of Russian Poland, in the government of
Siedlce, 16 miles to the east of the government capital,'
on the railway between Warsaw and Brest-Litovskiy, It
is first mentioned in the year 1390 as a feudal dominion
of King Yaghello. After frequently changing hands it
became the i^iroperty of the Czartoryski, and afterwards
of the Potockj family, whose palace is still to be seen in
the town. Its 10,000 inliabitants — half of whom are
Greek nonconformists, and half Jews and Poles — carry
on some trade in bristles, and pursue minor industries. '
MIERIS, the name of a family of artists who practise{i
painting at Leyden for three generations in the 17th and
18th centuries.
I. Frans van JIiekis, the elder, son of Jan van Mierls,*
a goldsmith and diamond setter, was born, according to,
Houbraken, at Leyden on the 16th of April 1635, and
died there on the 12th of March 1681. His father wished
to train him to his own business, but Frans preferred
drawing to chasing, and took service with Abraham Tor-
envliet, a glazier who kept a school of design. As often
happens,*- the youth's style was influenced by his earliest
surroundings. In his father's shop he became familiar
with the ways and dress of people of distinction. His
eye was fascinated in turn by the sheen of jewellery and
stained glass ; and, though ho soon gave up the teaching
of Torenvliet for that of Gerard Dow and Abraham van
den Tempel, he acquired a manner which had more of the
finish of the exquisites of the Dutch school than of tha
breadth of the disciples of Rembrandt. It should be
borue in mind that he seldom chose panels of which tho
size exceeded 12 to 15 inches, and whenever his name ia
attached to a picture above that 3i2e we may surely assign
it to his son Willem or to some other imitator. .Unlike
Gerard Dow when ho first left Rembrandt, or Jan Steen
when he started on an independent career, he never ven-
tured to design figures as large as life. Characteristic of
his art in its minute proportions is a shiny brightness and
metallic polish. Tlie subjects which he treated best are
those in wliich he illustrated the habits or actions of the
wealthier chsses ; but he sometimes succeeded in homely
incidents and in portrait, and not unfrequently he ven-
tured 00 allegory. He repeatedly painted the satin skirt
which Terburg brought into fashion, and he often rivalled,
Terburg in the faithful rendering of rich and highly-
coloured woven tissues. But he remained below Terburg
and Mctzu, because he had not their delicate perception of
harmony or their charming mellowness of touch and tint,
and he fell behind Gerard Dow, because he was hard and
had not his feeling for effect by concentrated light and
shade. In the form of his composition, wliich sometimea
represents tho framework of a window enlivened with
M i G — M I G
289
greenery; And adornod with bas-reliets within wnlcn figures
are seen to the waist, his model ia certainly Gerard Dow.
It has been said that he possessed some of the humour of
Jan Steen, who was his friend, but the only approach to
hamour in any of his works is the quaint attitude and
look of a tinker in a picture at Dresden, who glances know-
ingly at a worn copper kettle which a maid asks him to
mend.
It is a question whether Houoraken has truly recorded
this master's birthday. One of his best-known pieces, a
party of ladies and gentlemen at an oyster luncheon in
the hermitage at St Petersburg, bears the date of 1650.
Celebrated alike for composition and finish, it would
prove that Mieris had reached his prime at the age of
fifteen. Another beautiful example, the Doctor Feeling
a Lady's Pulse in the gallery of Vienna, is dated 1656 ;
and Waagen, in one of his critical essays, justly observes
that it is a remarkable production for a youth of twenty-
one. In 1657 Mieris was married at Leyden in the pre-
sence of Jan Potheuck, a painter, and this is the earliest
written record of his existence on which we can implicitly
rely. Of the numerous panels knomi to the writer of
these lines, twenty-nine at least are dated, — the latest
being an allegorj', long in the Ruhl collection at Cologne,
illustrating the kindred vices of drinking, smoking, and
dicing, in the year 1680.
Mieris had numerous and distinguished patrons. He
received valuable commissions from Archduke Leopold, the
elector-imlatine, and Cosmo III., grand-duke of Tuscany.
His practice was large and lucrative, but never engendered
in him either carelessness or neglect. If there be a differ-
ence between the painter's earlier and later work, it is that
the former was clearer and more delicate in flesh, whilst the
latter was often darker and more livid in the shadows.
When he died his clients naturally went over to his son
.Willeni, who in turn bequeathed his painting-room to his
«on Frans. But neither WUlem nor Frans the younger
equalled Frans the elder.
II. WnxEM VAX Mieris (1662-1747), son of Frans.
His works are extremely numerous, being partly imita-
tions of the paternal subjects, or mythological episodes,
which Frans habitually avoided. In no case did he come
near the excellence of his sire.
in. Feaxs VAX Mieris the younger (1689-1763) also
lived oil the traditions of his grandfather's painting-room.
The picturc3 of nil tbe generations of the Mieris family were suc-
cessfully imitated liy A. D. Siiajiliaaii, who lived at Lcipsic nad
was iiatioiiized by the court of ApUalt-Dessnu. To those who would
rtudy hi.-i deceptive form of nrt a visit to the collection of Wbrlitz
neftr Dossnu may nffoi-d iustructiou.
MIGXARD,PiERRE (1610-1695), caUed— to distinguish
him from his brother Nicholas — Le Romain, was the chief
French iiortrait-painter of the 17th century. He was born
at Troyes in 1610, and came of a family of i>ainters. In
1630 he left the studio of Simon A'ouet for Italy, where
he sjient twenty-two years, and made a reimtation which
brought him a summons to Paris. Successful with his
portrait of the king, and in favour with the court, Mignard
jiitted himself against Le Brun, declined to enter the
Academy of which he was the head, and made himself the
centre d opiwsition to its authority. The history of this
struggle is most imix>rtant, because it was identical, as
long as it lasted, with that between the old guilds of
France and the new body which Colbert, for political
reasons, was determined to support. Shut out, in spite of
the deserved success of his decorations of the cupola of
Val de Grace (1664), from any great share in those public
worte the control of which was the attribute of the new
Academy, Mignard was chiefly iictive in jxjrtraiture.
Tiirenne, Bossuet, Maintenon (Louvre), La Valliire, Sevign^,
Montesi»n. Descartes f Castle Howard), all the beauties
and celebrities of his day, sat to him. His readiness and
skill, his happy Instinct for grace of arrangement, atoned
for want of originality and real power. With the death of
Le Brun (1690) the situation changed; Mignard deserted
his allies, and succeeded to all the posts held by his
opponent. These late honours he did not long enjoy; in
1695 he died whilst about to commence work on the cupola
of the Invalides. His best compositions have been en-
graved by Audran, Edelinck, JIasson, Poilly, and others.
MIGNOKETTE, or Migxoknette (i.e., "Uttle dai^
ling"), the name given to a popular garden flower, the
Reseda odorala of botanists, a " fragrant weed," as Cowper
calls it, highly esteemed for its delicate but delicious perfume.
The mignonette is generally regarded as being of annual
duration, and is a plant of diffuse decumbent twiggy habit,
scarcely reaching a foot in height, clothed with bluntish
lanceolate entire or three-lobed leaves, and bearing longish
spikes — technically racemes — of rather insignificant flowers
at the ends of the numerous branches and brancUeta.
The plant thus naturally assumes the form of a low densa
mass of soft green foliage studded over freely with the
racemes of flowers, the latter unobtrusive and likely to be
overlooked until their diffused fragrance compels attention.
The native country of the original or typical mignonette
has sometimes been considered doubtful, but according to
the best and latest authorities it has been gathered wild oa
the North African coast near Algiers, in Egy])t, and in
Syria, As to its introduction, a MS. note in the library
of Sir Joseph Banks records that it was sent to England
from Paris in 1742 ; and ten years later it appeara to have
been sent from Leyden to Philip MUler at Chelsea. Though
originally a slender and rather straggling plant, there are
now some improved garden varieties in which the growth
is more compact and vigorous, and the inflorescence bolder,
though the odour is perhaps less penetrating. The small
six-petalled flowers are somewhat curious in structure : the
two upper petals are larger, concave, and furnished at the
back with a tuft of club-shaped filaments, which gives
them the appearance of being deeply incised, while the two
lowest petals are much smaller and undivided ; the most
conspicuous part consists of the anthers, which are
numerous and of a brownish red, giving the tone of colour
to the inflorescence. In a new variety named Golden
Queen the anthers have a decided tint of orange-yellow,
which imparts a brighter golden hue to the plants when
in blossom. A handsome proliferous or double-flowered
variety has also been obtained, which is likely to be a very
useful decorative plant, though only to be propagated by
cuttings ; the double white flowers grow in large massive
panicles (proliferous racemes), and are equally fragrant
with those of the ordinary forms.
^Vhat is called tree mignonette in gardens is due to tlie skill of
\.ic cultivator. Though practically a British annual, as already
noted, since it flowers abundantly the first season, and is utterly
destroyed by the nutnmnnl frosts, and though recorded as being
annual in its native habitat by Desfontaines in the Flm-a AtJantioa^
mignonette, like many other plants treated in England aa
nuals, will continue to grow on if kept in a suitable teniperaturo.
cr, the life of certain plants of this semiannual chai-acter
may be prolonged into a seoona season if their flowering and seeding
are pei-sistently prevented. In applying these facts to the pro-
duction of tree mignonette, the gardener grows on the young
plants under glass, and prevents their flowering l)y nipping olTthe
blooming tips of the shoots, so that they continue their vegetative
gi'owth iuto the second season. The young plants are at first sup,
ported in an erect position, the laterals being removed so as to
secure clean uinight stems, and then at the height of one or two
feet or more, as nmy be desired, o head of branches is encouraged
to develop itself. In this way very large plants can be prodnceo.
For orainary pnqxjses, however, other plans are adopted. In the
open bordei-s of the flower garden mi^uoueite is usually sown in
spring, and iu great nort takes care of UcPlf ; but, being a favourite
either lor window or balcony culture, and on account of its fragrnnc*
a welcome inmate of town conservatories, it is also very extfneively
XVL — 37
290
M I G — i\I I L
grown as r. ).:'•. j/i.nt, -jj'l f.a- m idat f 3rp&scs with this ohjcct it is
gown in pins in tin? itutuirn, and tliiiuiej out to cive the p1ant3
requisite siiace, since it docs not transplant well, and it is thereafter
specially ^rown in pita protected fiom frosts, and marketed when
just arriving at the blooming stage. In this way hundreds of
thousands, probably, of pots of blooming mignonette are raised and
disposed of year by year.
In classifying the odours given off by plants Rimmel ranks the
mignonette in the class of which he makes the violet the type; and
Fee adopts the same view, referring it to his class of *' iosmoida "
along with the violet and wallllower.
The name is sometimes, but it would appear less correctly, written
mignionette. The genus Reseda contains, some other interesting
and useful species, — among them the Rtscda Luicola, which is
commonly called dyer'a-weed and weld, and yields a valuable
yellow dye.
MIGUEL, Maria Evaeist (1802-1866), usually known
as Don Miguel, whoso name is chiefly associated with his
pretensions to the throne of Portugal, was the third son of
King John VI. of Portugal, and of Carlotta Joachima, one
of the Spanish Bourbons ; he was born at Lisbon on
October 26, 1802. In 1807 he accompanied his parents
lin their flight to Brazil, where he was permitted to grow
iTip a spoiled child and a worthless youth ; in 1821, on his
return to Europe, it is said that he had not yet learned
to read. In 1822 his father swora fidelity to the new
Portuguese constitution which had been proclaimed in his
absence ; and this led Carlotta Joachima, who was an
absolutist of the extremest Bourbon type, and otherwise
hated her husband, to resolve to seek his dethronement in
favour of Miguel her favourite son. The insurrection^
which ensued (see Portooal) resulted in her relegation to
the castle of Queluz and the exile of Miguel (1824), who
spent a short time in Paris and afterwards lived in Vienna,
where he came under the teaching of Jletternich. On the
sudden death of John VI. in Jlay 1826, Pedro of Brazil,
his eldest son, renounced the cron'n in favour of his
daughter JIaria da Gloria, on the understanding that she
should become the wife of Miguel. The last-named
accordingly swore allegiance to Pedro, to Maria, and to
the constitution which Pedro had introduced, and on this
footing was appointed regent in July 1827. He arrived
in Lisbon in February 1828, and, regardless of his
promises, dissolved the new Cortes in March ; having
called together the old Cortes, with the support of the
reactionary party of which his mother was the ruling
spirit, he got himself proclaimed 'sole legitimate king of
Portugal in July. The power which he now enjoyed he
iwielded in the most tyrannical manner for the repression
of aD liberalism, and his ))rivate life was characterized
by the wildest excesses. The public opinion of Europe
became more and more actively hostile to his reign, and
aiter the occupation of Oporto by Don Pedro in 1832, the
destruction of MigHel's fleet by Captain (afterwards Sir
Charles) Napier off Cajje St Vincent in 1833, and the
victory of Saldanha at Santarem in 1834, Queen Christina
pf Spain recognized the legitimate sovereignty of Maria,
ind in this was followed by France and England. Don
Miguel capitulated at Evora on May 29, 1834, renouncing
all pretensions to the Portuguese throne, and solemnly
promising never thenceforward to meddle in Peninsular
affairs. He lived for some time at Rome, where he en-
joyed papal recognition, but afterwards retired to Bronn-
tach, in Baden, where he died on November 11, 18fi6.
MIGULINSKAYA, a Cossack village (aanitm) of Russia,
in the gosernment of the Don Cossacks, and in the district
of Ust-Medvyeditsa, 79 miles to the west of that town, on
the left bank of the Don. It is one of the largest and
Wealthiest stanitsas of the government, and has 20,600
inhabitants, who axff engaged in agriculture and stock-
breeding, and In the export of agricultural produce.
MIKHAILOVSKAYA, a Cossack village (stanitsa) of
tiasaia, in the government of the Don Co^^cks. and in the
district cf Khopcrsk, 14 miles to the north-west of
UoTipino, on the low left bank of the IChoper, which ia
inundated when the river is full. It has an important
fair, where Tartars from Astrakhan exchange furs and
cottons for manufactiu-ed and grocery wares imported from
central Russia ; the inhabitants of the district also sell
corn, cattle, and plain woollen stuffs. Population, 18,000.
MILAN (the Latin Mtdiolanum, Italian Milano, and
German Mailand), a city of Italy, situated near the njiddle
of the Lombard plain, on the small river Olona, in 45° 27'
35" N. lat. and 9° 5' 45" E. long. It is 390 feet above'
the sea-level, and lies 25 mUes south of the Alps at Como,!
30 miles north of the Apennines, 20 miles east of the
Ticino, and 15 miles west of the Adda.
The plain around Milan is extremely fertile, owing at
once to the richness of the alluvial soil deposited by the
Po, Ticino, Olona, and Adda, and to the excellent system
of irrigation.' Seen from the top of the cathedral, the
plain presents the appearance of a va,st garden divided
into square plots by rows of mulberry or poplar trees.
To the 'east this plain stretches in an unbroken level,
as far as the eye can follow it, towards Venice and the
Adriatic ; on the southern side the line of the Apennines
from Bologna to Genoa closes the view; to the west rise
the Maritime, Cottian, and Graian Alps, with ilonte Viso
as their central point ; while northward are the Pennine,
Helvetic, and Rha^tian Alps, of which Monte Rosa, the
Saasgrat, and Monte Leone are the most conspicuous
features. In the plain itself li-e many small villages ;
and here and there a larger town like Monza or Saronno,
or a great building as the Certosa of Pavia, makes a white
point upon the greenery.
The commune of Milan consists since 1873 of the city
within the walls (area 1513 acres) and the so-called Corpj
Santi' without the walls (area 15,415 acres). The popu-
lation of the whole area increased from 134,528 in 1800
to 242,457 In 1861, 261,985 in 1871, and 321,839 in
1881, — the city within the walls contributing 110,884 in
1801, 196,109 in 1861, 199,009 in 1871, and 214,004
in 1 88 1. The climate is very variable ; there is a diff«rence
of 4 1 ° Fahr. between the extreme summer heat and winter
cold. The average number of wet days is 72, and of
snowy days 10 per annum.
Milan is built in a circle, the cathedral being the central
point. The city is surrounded by a wall 7 miles in
circumference, and immediately outside the wall a fine
broad thoroughfare malces the circuit of the city. The
streets inside are for the most part narrow and crooked j
the main streets are the Corso Vittorio Emanuele, -the
Strada S. Margherita, the Via ilanzoni, the Corso Porta'
Ticinese, and the Corso Porta Romana. There are few
piazzas of any size ; the largest is the Piazza del Duomo,
which has recently been extended, and the houses around
it modernized. To the west of the city is the open space
of the Foro Bonaparte and the Piazza d'Armi, with the
square keep of the Visconti castle, flanked by two granite
towers, between them. The castle was partly destroyed
in 1447 by the^Ambrosian republic, rebuilt by Francesco
Sforza, enlarged by the Spanish governors, and taken by
Napoleon in 1800, when the outer fortifications were razed
to the ground, and the walls left as they now are. North
of the I'iazza d'Armi is the modern cemeter)-, with a special
building and njipaxatus for cremation, erected in 1876.
Among the buildings of Milan the most important is the
cathedral, begun under Gian Galeazzo Visconti, in I.'^SG.
It is built of brick cased in marble from the quarries which
Visconti gave in perpetuity to the cathedral chapter. The
• The name Corpi Santi (of doubtful origin) is also applied t« ^^^9
extrft-Euural portions of Oiemooa and Paria.
MILAN
291
n&uie of the original architect is not known, bat it is
certain that many German master masons were called to
Milan to assist the Italian builders. After St Peter's at
Rome and the cathedral of Seville the Duomo of Milan is
the largest church in Europe. It is 477 feet in length
and 183 in width; the nave is 155 feet high, the cupola
226 feet, and the tower 360 feet. The work was con-
tinued through many centuries, and after the designs of
many masters, notably of Amadeo, who carried out the
octagon cupola, and of Tibaldi, who ornamented the
doors and windows of the facade in the 16th century. The
work was finished, under Napoleon, in 1805. lie style
is Gothic, though its purity is destroyed by the introduc-
tion of Romanesque windows and portals on the fa5ade.
The form of the church is that of a cross. Inside there
are double aisles, and aisles in the transepts. The roof is
Flau of Milan.
9. Pal. Deccariiu
10. S. Fcdclc
11. Teutro d. CanDobl&na,
13. Caaa Uboldl.
13. Pal. deUa Raglone.
14. Conserv. dl Muaica.
15. Teatro deUa Scala.
16. Casino del MeixanU.
17. Hotel RelchtTiniin.
18. Grand Hotel Itoyal.
19. Marino,
20. Hotel de la VDle.
21. Hotel Gran Btetagnt.
22. Ca*a Oripo.
23. Gallerla VlttOTio
1. Ffazza del Teatro.
t. Piazza del Uercanti.
8. 8. Anj^lo.
C Oapedaie delle Fate-
bcne SoTelle.
I. Ospedale del Fate bene
FratellL
<. Cusa Samoylotr,
7. S. Maria del Carmine.
a. Pal. de Brera.
supported by fifty-two columns, with canopied niches
for statues instead of capitals. The windows of the tribune
contain brilliant painted glass. To the right of the
entrance is the tomb of Archbishop Heribert, the champion
of Milanese liberty; next to that is the tomb of Otho
Visconti, founder of that family as a reigning house, and in
the right transept the monument of Giacomo dei Medici,
the corsair of Como, brother of Pope Pius IV. and uncle
to Saint Carlo Borromeo. Under the dome, in a crypt,
lies the embahned body of this cardinal saint (1538-84),
canonized for his good deeds during the great famine and
plague of 1576. The body is contained in a silver
sarcophagus faced with rock-crystaL The roof of the
cathedral is built of blocks of white marble; and the
various levels are reached by staircases carried up the
buttresses ; it is ornamented with turrets, pinnacles, and
two thousand statues.
There are four other churches of interest in Milan. S.
Ambrogio, the oldest, was founded by St Ambrose in
the 4th :entury. on the ruins of a temple of Bacchus. It
is remarkable for its fine atrium, and inside for the
mosaics in the tribune, dating from the 9th century, and
for the " pala " or plating of the high altar, a curious and
ancient specimen of goldsmith's work. S. Maria delle
Grazie is a Dominican church of the 15th century. The
cupola, vrith sixteen sides wrought in terra-cotta, is attri-
buted to Bramante. S, Gottardo is now built into the
royal palace, and only the apse and the octagonal campanile
remain. The latter, a beautiful example of early Lom-
bard terra-cotta work, was biiilt by Azzone Visconti in
1336, and was the scene of the murder of Giovanni Maria
Visconti in 1 4 1 2. The small church of San Satiro, founded
in the 9th century, was rebuilt by Bramante in the 15th ;
the sacristy is one of that master's finest works.
The royal and archiepiscopal palaces are both worthy
of note. The former stands on the site of Azzone Vis-
conti's palace, and the present building was the viceregal
lodge of the Austrian governors. It contains one fine
hall with a gallery supported by caryatides. The Broletto,
or town-hall, was built by Filippo Maria Visconti for his
general Carmagnola, in 1415, who, however, never Eved in
it. The Great Hospital is a long building with a fine
facade in terra-cotta from the designs of the Florentine
Antonio Averlino; it dates from the reign of Francesco
Sforza (1456), and can accommodate 2400 patients. Among
the modem buildings the most remarkable are the Arco
della Pace, which stands at the commencement of the
Simplon road (begun in 1804 by Napoleon, finished in
1833 under the Austrians), and the great GraUeria Vittorio
Emanuele, connecting the Piazza del Duomo with the
Piazza della Scala — a graceful glass-roofed structure 320
yards long, 16 yards wide, and 94 feet high, built in
1865-67 at a cost of 320,000 Ure (£12,800). The
Milanese are justly proud of this popular promenade, as the
finest of its kind in Europe ; and in the best of their four
considerable theatres — the Scala, built in 1778 on the
site of a church raised by Beatrice Soala, wife of Bemabd
Visconti — they also possess the largest theatre in Europe,
with the single exception of the S. Carlo at Naples.
Milan is rich in works of art. It has been the home of
many excellent sculptors and architects, among others of
Amadeo and of Agostino Busti, known as Bambaia, — whose
work may be seen in the cathedrals of Como and Milan, in
the Certosa of Pavia, and in the terra-cotta buildings of the
Lombard towns. Later on, towards the close of the 15th
century, the refined court of Lodovico Sforza attracted
such celebrated artists as Bramante the architect, Gaffurio
Franchino the founder of one of the earliest musical
academies, and Leonardo da Vinci, from whose school
came Luini, Boltraffio, Gaudenzio Ferrari, and Oggiono.
In still more recent times Beccaria (17^8-94) as a jurist,
Monti (1754-1828) as a poet, and Manzoni (1785-1873)
as a novelist, have won for the Milanese a high reputation
in the field of letters
The picture gallery of the Brera is one of the finest in
Italy. It possesses Raphael's famous " Sposalizio," and
contains many frescos by Luini, Gaudenzio Ferrari, and
Bramantino, The Venetian school is particularly well
represented by works of Paolo Veronese, Paris Bordone,
Gentile BelUni, Crivelli, Cima da Conegliano, Bonifazio,
Moroni, and Carpaccio, Luini may also be studied in the
church of Monastero Maggiore, a large part of whose walls
he painted in fresco. In the archicological museum, on the
ground floor of the Brera, are preserved many interesting
monuments, among others the tomb of Beatrice della
Scala and the equestrian monument of her husband
BemabJi Visconti, as well as the most exquisite sepulchral
monument of Gaston de Foix, the work of Agostino Busti
The library of the Brera contains upwards of 200,000
volumes, inclndinsr some important Venetian chronicles,
392
MILAN
but it 13 not so rich in MSS. as tlie celebrated Ambrosian
library, for wbich see Libeaeies, voL xiv. p. 531.
jiffric%dture.—Th6 district of Milan is renowned for Ita excellent
agriculture. It may be divided into two regie is, where diffijrent
systems of farming are pursued and different crops produced. The
first region lies on the lower slopes of the Alps, where they sink
into the plain. This is called the dry Milanese, for it is watered
by torrents onl^,, which have worn themselves too deep a bed to
allow of irrigation, and the peasants are obliged to collect the rain-
water in large mud-lined tanks called "poppe." The soil is for
the most part thin and light, and is frequently washed down the
incline into the plain ; in some parts it is only kept in its place by
stone walls reared at great cost The farms are smaller here than
in the lower plain, and are let on a system which is a compromise
between the mezzadria, which once obtained in the distnct, and
regular leases. The tenant pays a money rent for the house ; and
for the land he either pays in kind or in a money equivalent,
supplemented by labour given to the landlord. In caSes where
vines or fruit trees are grown, the landlord supplies and maintains
them till they come into fruit The landlord carries out all
improvements, and the tenant holds the farm at his pleasure.
The rotation of cropping is for three years. The value of these
farms varies greatly, ranging from 7 to 14 lire the pertica (1000
squai'e yards). The district produces maize and wheat in abund-
ance, a little flax and mUlet, apples, and wine. The second
dgricultural district is that which lies in the plain ; it is called the
wet Milanese, from the elaborate system of irrigation which makes
the meadows yield a constant succession of crops. The plain is
traversed by innumerable canals at various levels, crossing one
another on bridges, or by siphons, so that the peasant can flood
his fields at any moment The system is as old as the 12th
century; it was improved by Leonardo da Vinci, and is now the
most perfect network of irrigation in Europe. The farms vary in
extent from 1500 to 4500 pertichc. They are let upon leases for
nine, twelve, or fifteen years, at rents ranging from 8'50 to 12"50
lire the pertica, while those near a city may bring from 16 to 20
lire. The rotation of cropping is five-yearly. The meadows yield
four crops of grass in the year ; the first three — the maggengo, the
agostino, and the terzuolo— are cut, the fourth is grazed off.
where the ground is perfectly flat and water can stagnate, rice is
gi'own ; this crop is continued for four years in succession, then
the land is rested with cereals and grass. The other crops are
maize and wheat. But the chief occupation is the supply of dairy
Eroduce. The cows are bought in tlie Swiss cantons of Uri, Zug,
ucerne, and Schwyz, the last furnishing the best milkers. The
cheese called Parmesan comes from the Milanese ; and the rich
cheese, made of unskimmed milk, known as Stracchlr.D, is made
principally at the %'illage of Gorgouzola, 12 miles east of Miian.
Industries. — The industries of this district have increased veiy
i-apidly since the union of Italy, and the city is now the chief
commercial centre iu North Itnly. The principal industry of
Milan and the Milanese is the production and manufacture of silk.
For feeding the worms mulbeiTy trees are largely cultivated on the
plain ; and the distiicb counts upwards of 200 factories, where the
Bilk thread is unwound from the cocoonj, yielding 4,000,000 lb of
raw silk in the year. Some of this is exported to France for
manufacture, but the Milanese can now almost rival their
neighbours in the production of silk stuffs, velvets, and brocades.
Cotton is manufactured at Saronno and Lcgnano, fustian at Busto,
lineu at Cassano, combs at Burlando, and porcelain and carriages
of very excellent woi'kmanship in Milan itself.
History. — Rellovesus, king of the Celts, who crossed the Aips
when Tarquinius Priscus was king in Rome, is the traditional
founder of Milan. The city became the capital of the Insubrian
Gauls, and was taken by the Romans in 222 b,o. As a Roman
municipium it continuecl to increase in magnificence and import-
ance ; and under Constantino it was the seat of the imperial vicar
of the West Under Theodosius, in the 4th century, Milan, to
judge from Ausonius's description {Ordo Nob. Urbitim, v.), must
nave been rich in temples and public buildings. Theodosius died
at Milan after doing penance, at the bidding of St Ambrose, for
his slaughter of the iwople of Tlicssalonica. Ambrose is still
■venerated in Milan as tne founder of the Milanese church and the
compiler of the Ambrosian rite, which is still in use throughout
the diocese. After his death the period of invasions begins ; and
Milan felt the power of the Huns under Attila (4521, of the
Heruli under Odoacor (476), and of the Goths under Theodoric
(493). "When Belisarius was sent by Justinian to recover Italy,
Dfttius, the archbishop of Milan, joined him, and the Goths were
expelled from the city. But Uraia, ucnhew of Vitigis the Gothic
king, subsequently assaulted and retook the town, after n bravo
resistance. Uraia destroyed the whole of Milan in 539 ; and hence
it is that tliis city, once so important a centre of Roman civilization,
possesses so few remains of antiquity. Naracs, in his campaigns
against the Goths, had invited other barbarians, the Lombards, to
his aid. They camo in a body under Alboiu, their king, in 508,
and were soon masters of Iforth Italy, and entered Milan the year
following. Alboin established his capital at Pavia, and lUlan
remained the centre of Italian opposition to the foreign conquest
The Lombards were Arians, and the archbishops of Hiian from
the days of Ambrose had been always orthodoi. Though thft
struggle was unequal, their attitude of resolute opposition to the
Lonil)ard8 gained for them great weight among the people, who
felt that their archbishop was a power around whom they might
gather for the defence of^ their liberty and religion. All the innate
hatred of the foreigner went to strengthen the hands of the
archbishops, who slowly acquired, in addition to their spiritual
authority, powers military, executive, and judicial. These iwwen
they came to administer through their delegates, called viscounts.
When the Lombard kingdom ^U before the Franks under Charles
the Great in 774, the archbishops of Milan were still further
strengthened by the close alliance between Charles and the church,
which gave a sort of confirmation to their temporal authority, and
also by Charles's policy of breaking up the great Lombard fiefs and
dukedoms, for which he substituted the snialler counties. Under
the confused government of Charles's immediate successors the
archbishop was the only real power in Milan. But there were
two classes of difficulties in the situation, ecclesiastical and political;
and their presence had a marked effect on the development of the
people and the growth of the commune, which was the next stage
in the history of Milan. On the one hand the archbishop was
obliged to contend against heretics or cgainst fanatical reformers
who found a following among the people; and on the other, since
the archbishop was the real power in the city, the emperor, the
nobles, and the people each desired that he shoiUd be of their party ;
and to whichever party he. did belong he was certain to find
himself violently opposed by the other two. From these causes it
sometimes happened that there were two archbishops, and there-
fore no central control, or no archbishop at all, or else an archbishop
in exile. The chief result of these difhculties was that a spirit of
independence and a c.-*pacity of judging and acting for themselves
was developed in the people of Milan. The termor of the
Hunnish invasion, in 899, further assisted the people in their pro-
gress towards freedom, for it compelled them .to take arms and to
fortify their city, rendering Milan more than ever independent
of the feudal lords who lived in their castles in the country.
The tyranny of these nobles drove the peasantry and smaller
vassals to seek the protection for life and property, the equality of
taxation and of justice, which could be found only inside the walled
city and under the rule of the archbishop. Thus Mibn grew
populous, and learned to govern itself. Its mhabitants became for
the fii-st time Milanese, attached to the standard of St Ambrose, —
no longer subjects of a foreign conqueror, but a distinct people^
with a municipal life and prospects of their own. For the further
growth of the commune, the action of the great archbishop Heri-
bert, the establishment of the carroccio, the development of
Milanese supremacy in Lombardy, the destruction of Lodi, Come,
Pavia, and other neighbouring cities, tie exhibition of free spirit
and power in the Lombard league, and the battle of Legnano, see
the article Italy. See also Lombards.
After the battle of Legnano, in 1174, althongn me Lombard cities
failed to r^ap the fruit of their united action, and fell to mutual
jealousy once more, Milan internally began to grow in material
prosperity. After the peace of Constance (1183) the city walls
were extended ; the arts flourished, each in its own quarter, un^er
a syndic who watched the interests of the trade. The manufacture
of armour was the most important industry. During the struggles
with the emperor Barbarossa, whei> freedom seemed on the point
of being destroyed, many Milanese vowed themselves, their comIs,
and their families to the Virgin should their city come safely out
of her troubles. Hence arose the powerful fraternity of the
"Umiliati," who established their headquarters at the Brcra, and
began to develop the wool trade, and subsequently gave the first
impetus to the production of silk. From this period also date the
irrigation works wliich render the Lonbard plain a fertile garden.
The government of the city consisted of (A) a parlnmento or con*
siglio gi"ande, including all who possessed bread and wiiio of their
own, — a council soon found to bo unmanageable owing to its sixe,
and reduced first to 2000, then to 1600, and finally to 800 mem-
bers ; (B) a credenza or committee of twelve members, ejected
in the grand council, for the despatch of urgent or secret busineaa :
(C) the consuls, the executive, elected for one year, and compelled
to reuort to the great council at the term of their olScc. The way
in which the burghen used their liberty and powers, secured bv
the peace of Constance, in attacking tlie feudal nobility ; how the^
compelled the nobles to come into the city and to abandon their
castles for a certain portion of the year ; how the war between the
two classes was continued inside the city, ri'sulting in the establiali-
mont of the podesU\ ; and the nature and limits of this office, — all
this has been cxplninrd in the article Italy.
This bitter and wellbabnccd rivalry between the nobles and tbe
people, and the endlo<.s danger to which it exposed the city owing
to tlic fuel tliat the nobles wci-o always ready to claim the protec-.
M I L — MIL
293
tion of their feudal chief, (3i» emperor, hrooght to the front two
aoble funilies u protagonists of the contending factions,— the
Torriani of Valsessina, and the Yisoonti, who derived their name
from the office they had held nnder the archbishops. After the
battle of Cortcnova, in 1237, where Frederick II. defeated the Guelf
array of the Milanese and captured their carroccio, Pagano della Torre
rallfed and saved th6 remnants of the Milanese. This act recom*
mended him to popular favour, and he was called to the government
of the city, — but only for the distinct purpose of establishing the
"catasta, ' a property tax which should fall with equal incidence on
every citizen. This was a democratic measure which marked the
party to which the Torriani belonged and rendered them hateful
to the nobility. Pagano died in 1241. His nephew Martino fol-
lowed as podest^ in 1256, and in 1259 as signore of Milnn, — the
tot time such a title was heard in Italy. The nobles, who had
Sthered round the Visconti, and who threatened to bring Ezzelino
Romano, the Ghibelline tyrant of Padu,-. into the city, were
defeated by Martino, and nine hundred of their number were
captured. Martino was followed by two other Torriani, Filippo
bis brother (1263-65) and Napoleone his cousin (1265-77), as lords
of Milan. Napoleone obtained the title of imr>erial vicar from
Rudolph of Hapsburg. But the nobles under the Visconti had been
steadily gathering strengtli, and Napoleone was defeated at Besio
in 1277. He ended his life in a wooden cage at Castel Baradello
above Coroo.
Otho Visconti, archbishop of Milan (1262), the victor of Desio,
became lord of Milan, and founded the house of Visconti, who ruled
the city — except from 1302 to 1310— till 1H7, giving twelve lords
to Milan. Otho (1277-95), Matteo (1310-22), Galeazzo (1322-28),
Alio (1328-39), Lucchino (1339-49), and Giovanni (1349-54) fol-
lowed in succession. Giovanni left the lordship to three nephews —
Matteo, Galeazzo, and Bernabi. Matteo was killed (1355) by his
brothers, who divided the Milanese, Bemab6 reigning in Alilan
(1354-85) and Galeazzo iu Pavia (1354-78). Galeazzo left a son,
Gian Galeazzo, who became sole lord of Alilan by seizing and im-
prisoning his uncle Bernab6. For an account of this most powerful
prince see Italy. It was under him that the cathedral of Milan
and the Certosa of Pavia were begun. He was the first duke of
Milan, having obtained that title from the emperor Wenceslaus.
His sons Giovanni Maria, who reigned at Milan (1402-1412), and
FUippn Marin, who reigned at Pavia (1402-1447), succeeded him.
In 1412, on his brother's death, Filippo united the whole duchy
onder his solo rule, and attempted to carry out his father's policy
of agCTandizement, but without success.
Filippo was the lass male of the Visconti house. At his death a
republic was proclaimed, which lasted only three years. In 1450
the general Francesco Sforza, who had married Filippo's only child
Bianca Visconti, became duke of Milan by right of conquest if by
any right. Under this duke the canal of the lilartesana, which
connects Milan with the Adda, and the Great Hospital were carried
out. Francp!»co was followed by five of the Sforza family. His son
Galeazzo Maria (1466-76) left a son, Gian Galeazzo, a minor, whose
guanliaii and uncle Lodovico usuiped the duchy (1479-1500). Lodo-
Tico was captured in 1500 by Louis XII. of France, and Milan
remained for twelve years under the French crown. In the partial
settlement which followed the battle of Ravenna, Massimiliano
Sforza, a protege of tlie emperor, was restored to the throne of Milan,
and held it by the help of the Swiss till 1515, when Francis 1.
of France reconquered the Milanese by the battle of Marignano,
and Massimiliano resijmed the sovereignty for a revenue from France,
This arrangement did not continue. Charles V. succeeded the
emj^ror Maximilian, and at once disputed the possession of the
Milanese with Francis. In 1522 the imperialists entered Milan and
proclaimed Francesco Sforza (son of Lodovico). Francesco died in
1535, and with bim ended the house of Sforza. From this date till
the war of the Siwnish succession (1714) Mil.m was a dependency of
the Spanish crown. At the ck>so of that war it was handed over
to Austria ; and under Austria it remained till the Napoleonic
campaign of 1796. For the results of that campaign, and for the
history of Italian progress towaiils independence, in which Milan
played a prominent part bj- opening the revolution of 1848, the
reader is referred to the articJe Italy. The Lombard campaign of
1859, with the battles of Solferino and Magenta, finally made Milan
a part of the kingdom of Italy.
hleralnrt.—rkm Vcnl, Siordi dl UUam ; Corio. Sloria il tlitano ; C«nlb,
iHitHratiomt Orantt* del Lombardo Viiielo\ Itie Mtlaiieso chroniclei-s In Mura-
fort's B<r. ItaK Scrlptt)rn', Slimon<1l, Italian RepitbtUt; Feirdrt. Rit\>tutione tf
IXalta. Llln. Famlglieteltbrl, ir." Torriani," ■'Visconti." •' Sfoiza.'and'TrivulzU"
Muralorl. Aanall d'llalla ; Rallaro, Hlilarg a/ Iht MidJIe A^es ; and Uediolanum.
4 roll., 1S81. DonirldlM da Rlrl xivcs • coDtemjwraiy account of Slllan In the
IStll ccnlur}-. (H. F. B.)
3IILAZZ0, a city of Italy in the province of Messina
in Sicily, 20J miles west of ilessina, is built on the eastern
shore of the Bay of Jlilazzo, partly on the isthmus of the
promontory, Capo Milazzo, which divides it from the Bay
of Olivieri. It consists of an old or upper town protected
bj_ strong bosticned walls, and a lower. or_ modern town
outside of the enceinte. ~ The fine old castle is now tised
as a prison. Besides a certain amount of foreign cem-j
merce (37 vessels with a burden of 6707 tons entering in
1881, 93 -with 13,496 in 1863), Milazzo carries on a gaoi
coasting trade (194,366 tons in 1881, 40,138 in 1861);
and is one of the seats of the tunny-fishery. The com-
munal popujation increased from 10,493 in 1861 to 13,565
in 1881, and that of the city was 7427 in 1871
Milazzo is the ancient Mylte, a seaport and fortress founded tsf
the Zancheans (Messanians), which gives its name to the battle oC
the Klyleean plain in which the Mamertines were defeated by Hiero
in 270 B.O. In 1523 itwas the scene of an unsuccessful conspiracy
to transfer Sicily to the French. Captured by the Germans in 1718,
it was besieged by the Spaniards, but relieved by a Neapolitan and
English force. In July 1860 the defeat of the Neapolitans in the
vicinity, and the seizure of the fortress, formed almost the crown-
ing act of Garibaldi's victorious campaign. The Bay of Milazzo haa
been the scene of the defeat of the Carthaginian navy by Duilios
(260 B.O.), of Pompeius by Octavian's general Agrippa (36 B.C.X and
of the French and Messinian galleys by the Pisans (1268).
MILDEW (explained as " meal-dew " or, with ' more
probability, aa "honey-dew") is a popular name giTen
to various minute fungi from their appearance, and from
tire sudden, dew-like manner of their occurrence. Like
many other popular names of plants, it is used to denote
different species which possess very small botanical
affinity. The term is applied, not only to species be-
longing to various systematic groups, but also to snch
as follow different modes of life. The corn-mildew,
{he hop-mildew, and the vine-mildew are, for example,
parasitic upon living plants, and the mildews of damp linen
and of paper are saprophytes, that is, they subsist on
matter which is already dead. It is generally possible to
draw a distinct line between parasitic and saprophytie
fungi ; a species which attacks the living body of its host
does not grow on dead matter, and vice versa. This is true
so far as is known of perhaps all the higher fungi except
Stiprohgnia ferax (Gniith.), a parasite of freshwater
fishes (especially of the salmon), which also grows freely
on their dead bodies and on those of llie'^ &c. As regards
mildews in general, the conditions of life end growth are
mainly suitable nutrition and dampness accompanied by a
high temperature. The life-history of the same species of
mildew frequently covers two or more generations, and
these are often passed on hosts of different kinds. In
some cases again the same generation confines its attack
to the same kind of host, while in others the same genera-
tion grows on various hosts. For information regarding
fun^ generally see Fungus, vol. ix, p, 827.
The folloNving examples are of common occurrence.
The Com-Mildeii! {Fuectnia graminis, Pers., OrtJer
Uredinese). — This disease of our grain crops and of many
other grass plants is very widely distributed, like its hosts,
over the earth, and is by far the most important to man of
all mildews. Its life-history is passed in three generations
— two of them on the grass plants and one on the barberry.
In early spring the first generation is found on the dead
leaves and leaf-sheaths of grass plants (in which the
disease has hibernated), presenting to the naked eye the
appearance of thin black streaks. When examined with a
microscope these streaks are seen to consist of a great
number of minute two-celled and thick-walled teleutosporea
i reproductive bodies), each situated at the end of a stalk
tee A in fig. 2, vol. ix. p. 831). These have burst through
the epidermis of the plant from their origin on threads
among the tissues beneath. When they have been in
contact with excessive moisture for a few hours, each of
the 8pore<ells germinates by emitting a fine tube called a
promycelium, on which there are borne small round tUn-
walled sporidia (reproductive bodies). The sporidia are
easily detached and carried from place to place by the
wind, and on alighting on the leaves of a barberry pkot
2l»4
MI E — M I L
soon germinate by pushing out a small tube ivhich jjer-
forates the epidermis and thus gains access to the interior
of the leaf, where it branches copiously, and forms a mass
of thread-like tissue called mycelium. The germ-tubes of
sporidia are unable to enter the leaves, itc., of grass plants.
In from si.x to ten days this mycelium gives rise to Hask-
sh.iped bodies called .spermogonia (vol. ix. p. 831, fig. 2
B, sj>), immediately under the surface of the leaf (usually
the upper one), but breaking through it at the neck of the
'fla.sk, out of which there protrudes a bunch of hairs.
Within the flatsks are formed at the end of stalks many
exceedingly small oval bodies called spermatia, which escape
through the neck. 'The function of these bodies has not yet
been definitely made out, but that they bear a very strik-
ing resemblance to the male sexual organs of other fungi
there can be uo doubt. In the same leaves and on the same
mycelium there arise several days later numerous basin-
shaped bodies containing erect stalks, bearing at the apex
R number of round Kcidiospores (reproductive bodies) iu
vertical series (vol. ix. p. 831, fig. 2 B, a). These con-
stitute the second generation. On their escape they
germinate by emitting a tube which, if the host on which
they fall be a grass plant, .enters the leaf through one of
the stomata in the epidermis, and there by branching forms
a new mycelium. On this there soon appears, bursting
through the epidermis, a new generation consisting of round
or oval uredospores produced at the end of stalks (vol. ix.
p. 831, fig. 2 C). The uredospores constantly reproduce
this generation, and in such abundance that the grain crops
Li-e extensively ravaged by its attack. It is m this genera-
tion that the term mildew is po[iularly given to the fungus.
Later in autumn on the same mycelium the two-celled
teleutospores appear, and these after hibernating renew in
spring the life-history. This very remarkable cycle of
generations was first traced by Professor de Bary.
The Eop-MiUUw {Sphserothcac C'usta(/nci, Lev., Order Erysi-
ph-:x) U a para-sitic disease of the hop, though it is often to be
found ou many other plants, such ns Potaitilla, SpiraM, Epilolitiin,
balsams, cucumbers, dandelions, plantains, &c. The thread-Uko
mycelium appears on the young shoots and leaves of the hop in
white spots, which gradually extend and finally unite. This
mycelium bears many minute, round conceptacles (perilhecia) which
with their supporting threads are brown-coloured. "Within each
perithecium is found a somewhat oval body termed an aicus, con-
taining eight ascospores (reproductive bodies).
The Viiu:-MiUlcii) {Enjsiphc Tii(kcri, Berk., Order Erysiphem) is
known only iu one generation — called the oidium stage. Soon after
the flowering of the vine the attack takes place on the young leaves,
from which the thin white mycelium spreads rapidly to the older
leaves and twigs, which it does not appear to allcct so injuriously.
The chief damage is done to the grapes while they arc iu a very
immature condition. The mycelium which travels over the surface
sends down at intervals into the tissues shoit irregular protuber-
ances called haustoria, which perform for it the functions of roots.
Above these rise h'om the mycelium short stalks bearing each a single
oval spore at the apex. The disease spreads ou the same plant not
only by the extension of the myceliUm but by the scattering and
germination of the spores. Here no perithecia are known.
The Paper- MUdew\Asa>lriclia diarUiium, Uel k. , Order Erysiphae)
grows oil damp liaper, and therefore is saprophytic in its mode of
Ufe. It consists ut first of a branching falaineiitous mycelium on
which minute globular sjiores occur. Finally a round bi'own peri-
thecium is formed among the threads which appear as radiating
from it. Within the perithecium arc numerous linear asci contain-
ing each c row of dark elliiitic ascostiores.
For the Erysipli/:ic generally sec Fuxofs, vol. ix. p. 833.
MILETUS, an ancient city on the southern .shore of
the Latmic Gulf opposite the mouth of the Marauder.
Before the Ionic migration it was inhabited by the Carians
(Iliad ii. 876 ; Herod, i. 1 16) ; other authorities call the
origiual people Leleges, who aic always hard to distinguish
from Carians. The Greek settlers from Pylus under
Neleus mas.sacred all the men in the city, and built for
theiu-selves a new city on the coast. It occupied a very
favourable situation at the mouth of the rich valley of
the Mxander, and was the natural outlet for the trade
of .southern Phrygia (Hipponax, Ft: 45); it had four
harbours, one of considerable size. Its power extended
inland for some distance uii the valley of the Jheander,
and along the coast to the south, where it founded the city
of lasus. The trade with the Black Sea, however, was
the greatest source of wtalth to the Ionian cities. Miletua
Uke the rest turned its attention chiefly to the north, and
after a time it succeeded iu almost monopolizing the traffic.
Along the Hellespont, the Propontis, and the Black Sea
coasts it founded more than sixty cities — among them
Abydus, Cyzicus, Sinope, Dioscurias, rautieapa;uni, and
Olbia. All these cities were founded before the middle of
the 7th century ; and before 500 B.C. Miletus was decidedly
the greatest Greek city. During the time when the enter-
prise and energy of the seafaring population, the iiii'a.vrai,
raised Miletus to such power and wealth, nothing is known
of its internal history. The analogy of all Greek cities,
and some casual statements in later writers, suggest thai
the usual bloody struggles took place between the oligarchy
and the democracy, and that tyrants sometimes raised
themselves to supreme power in the city ; but no detail!
are knorni. Miletus was ecjiually distinguished at this early
time as a scat of literature. The Ionian epic and lyrio
poetry indeed had its home farther norlh ; philosophy anc)
history were more akin to the practical race of Miletun,
and Thales, Anaximander, Anaximenes, Hecatiuus, aL
belonged to thia city. The three Ionian cities of Caria-^
Miletus, Myus, and Priene — .spoke a peculiar dialect ol
Ionic'
^^^len the Mcrmnad kings raised Lydia to be a gre^t
ir^ilit^iry kingdom, Miletas was their strongest adversary.
AVii; >\as carried on for many years, till Alyattes concluded
a peace with Thrasybulus, tyrant of Miletus ; the ililesians
afterwards seem to have picaccahly acknowledged the rule of
Crtesus. On the Persian conquest Miletus jjasscd under a
new master ; it headed the revolt of 500 B.C., <£Dd was
taken by storm after the battle of Lade. Darius treated
it with peculiar severity, mas.sacred most of the inH^bitants,
transported the rest to Ampc at the moutti of the Tigris,
and gave up the city to the Carian,s. Henceforth the
history of Miletus has no .special interest ; it revived indeeil
when the Persians wereexi)ulled from the coast in 479 BC,
and was l town of commercial imjjortanee throughout the
Gra;co-Roman period, when it sharud in the general fortunes
of the Ionian cities under the rule'cf Atheniarj.s, Pwsians,
Macedonians, Pergamenian.s, and Tlomans in svKBcssion.
Its harbours, once protected by* Lade and the other
Tragusaan islands, were gradually silted up by the
Ma:ander, and Lade is now a hill some miles from tlio coast.
Ephesus took its place as the great Ionian harboiir in tho
Hellenistic and lioman times. It was tho scat of a
Christian bishopric, but its decay wa.s sure, and its site ia
now a marsh.
See Schiocdcr, Commettl. lie Jicb. .Vila.; SolJan, Xrr. Vila.
Comim-iil. ; Uayet, Mild H h Oolfc Lnhnir/iir; Head, "Early Elec-
trum Coins," in Numisin. C/iroii., vol. xvi,
MILFORD, a seaport, market-town, and contributory
parliamentary borough (one of the Pembroke district)
of Pembrokeshire, South Wales, Ls finely situated on
the north side of Milford Haven, about i? miles west-
northwest of Pembroke. The land-locked estuary of
llilford Haven stretches about 10 miles inland, with a
' The coinage of Militus during this early (leriod is an imiwrtant
subject ou account of the wide loniiiiertial coniiexioui. of the city.
The early clcctnim coinage belong, to the IMi'euicinn or Gneco-Asiatic
standard, which was iiitr»luce<l from I'liauicia and spread over niauj,
of the Ionian and Thrncian cillis through the inHucucc of Milesian
trade. Very archaic coins of Miletus, Kphesus, Cyiue, anil Sardis ars
known of this staiidaril, and at a somewhat later dale of t:hio«, Sainos,
Clnzomeno', Unipsacus, Abydus, and Cyzieus. Tli« liou it the ngaiu,
Milesian \yiv. uUna with a ntui builuii ur.aUove liim.
MIL" mi L
2^d
breadth of from 1 to 2 miles. In most places it iiasia
depth of from 15 to 19 fathoms, and, as it is- complete!;
sheltered by hills, vessels can ride in it at anchor in all
kinds of weather. The royal dockyard, founded at
Milford in 1790, was removed in 1811, and from that time
trade has been in a languishing condition. The town
possesses iron-works. The shipping trade is confined
chiefly to coasting vessels, but with the completion of new
docks, capable of receiving ve^els of the largest tonnage,
It is supposed that a considerable trade may be carried on
with America. The population of the urban sanitary dis-
trict in 1871 was 3252, and in 1881 it was 3813.
MILFORD, a post-village of the United States, in
Worcester county, Massachusetts, lies 34 miles southwest
of Boston, at the junction of the Milford branch of the
Boston and Albany Railroad with the Hopkinton, Milford,
and Woonsocket Railroad. It is one of the principal seats
of the boot manufacture in New England, and also pro-
duces large quantities of straw goods. The population
was 9310 in 1880.
MILICZ, or MiLiTSCH, of Kremsier, Moravia, was the
most influential among those preachers and ^TTiters in
M9ravia and Bohemia who during the 14th century paved
the way for the reforming activity of Huss and through
him for that of Luther. He was born about 1325, was
already in holy orders in 1350, in 1360 was attached to
the court of the emperor Charles IV., whom he accompanied
into Germany in that year, and about the same time also
held a canonry in the cathedral of Prague along with the
dignity of archdeacon. About 1363 he resigned all his
appointments that he might become a preacher pure and
simple ; he addressed scholars in Latin, and (an innovation)
the laity in their native Czech, or in German, which he
acquired for the purpose. The success of his labours in
reclaiming the fallen made itself apparent in the reforma-
tion of a whole quarter of the city of Prague. As he dwelt
more and more on ecclesiastical abuses and the corruption
of the clergy, and viewed them in the light of Scripture,
the conviction grew in his mind that the " abomination of
desolation " was now seen in the temple of God, and that
antichrist had come, and in 1367 he went to Rome (where
Urban V. was expected from Avignon) to expound these
views. He affixed to the gate of St Peter's a placard
announcing his sermon, but before he could deliver it was
thromi into prison by the Inquisition. Urban, however,
on his arrival ordered his release, whereupon he returned to
Prague, and from 1369 to 1372 preached daily in the Teyn
Church there. In the latter year the clergy of the diocese
complained of him to the papal court at Avignon, whither
he was summoned in Lent 1374, and where he died before
his case was decided. He was the author of a Libelltts de
Antichristo, written in prison at Rome, a series of Postillss
and Ledioiies Qitadrar/esimales in Latin, and a similar
series of Posdh in Czech.
MILITARY FROXTEER (German, MUitargrenze;
Slavonic, Granitza), a narrow strip of Austrian-Hungarian
territory stretching along the borders of Turkey, which
had for centuries a peculiar military organization, and from
1849 to 1873 constituted a crown-land. As a separate
division of the monarchy it owed its existence to the
necessity of maintaining during the 15th, 16th, and 17th
centuries a strong line of defence against the invasions of
the Turks, and may be said to have had its origin with
the estabUshment of the captaincy of Zengg by Matthias
Corvinus and the introduction of Uskoks (fugitives from
Turkey) into the Warasdin district by the emperor
Ferdinand I. By the close of the 17th century there were
three frontier " generalates " — Carlstadt, Warasdin, and
Petrinia (the k&t also called the Banal). After the defeat
of the Turkish power by Prince Eugene it waa proposed to
^Bolish tHe military' constitution of the frontier, bflt tSf
chaiSbejras succeisafuljy resisied byJae'mhabLtantsSJ Ih,-
nistncfl "" the fstner hanO, a nen" SlaVuuiau irontier di»-'
tnct was eslablished in 1702, and Maria Theresa extended
the organization to the march-lands of Transylvania (the
Szekler frontier in 1764, the W-allachian in 1766).'
As a reward for the service it rendered the Government
in the suppression of the Hungarian insurrection in 1848,
the Military Frontier was erected in 1849 into a crown-land,
^th a total area of 15,182 square miles, and a population
of 1,220,503. In 1851 the Transylvanian portion (1177
square miles) was incorporated with the rest of Transyl-
vania ; and in 1871 effect was given to the imperial decrea
of 1869 by which the districts of the Warasdin regiments
(St George and the Cross) and the towns of Zengg, Belovar,
IvaniJ, ic, were "provincialized" or incorporated with
the Croatian-Slavonian crown-land. In 1872 the Banat
regiments followed suit; and in 1873 the old military
organization was abolished in all the rest of the frontier.
Not till 1881, however, were the Croatian-Slavonian
march-lands completely merged in the kingdoms to which
they naturally belonged
The social aspect of the military frontier regime is interesting.
a. communal sj'stcm of land tenure natural to the old Slavoiiiana
was artificially kept In existence. The mark or plot of ground
assigned to the original family of settlers i"emained the property of
the familyassuch, andcouldnot be portioned out among the several
members. In this way the house-community, all under the rule
of the same house-father and house-mother (who were not neces-
sarily man and wife, nor the oldest members of the community),
aud all living within the same palisade, sometimes came to num-
ber two or three hundred persons. The "family" dined in a com-
mon hall, and after dinner discussed and settled matters affecting
the common weal. Eveiy man possessing real property in the
country, and capable of bearing arras, was liable to military service
from his twentieth year. The house-communities are now begin-
ning to avail themselves of the permissive partition laws, and
strangeiTs are free to come and acouire property in land. Watch-
towers with wooden clappers ana the beacons which flashed the
alarm along the whole frontier in a few hours are still features in
the landscape.
MILITARY LAW consists of tUe statute-s, rules of pro-
cedure, royal warrants, and orders and regulations which
prescribe and enforce the public obligations of the officers,
soldiers, and others made subject to its provisions. Its
essential purpose is the maintenance of discipline ; but it
also includes the administrative government of the military
forces of the state, more especially in the matters of enlist-
ment, service, and billeting. The term "martial law"
sometimes apphed to it is, as regards modern times at least,
a misnomer. For martial law as it is now understood
applies not only to military persons but to the civil com-
munity, and may be described generally as the abrogation
of ordinary law and the substitution for it of military
force uncontrolled save by what, in the discretion of the
commanding general, may be considered the necessity of
the case.
The military law of England in early times existed, like
the forces to which it applied, in a period of war only.
' By 1S48 the following had come to be the division of the Militaiy
Frontier:— (1) The Carlstadt (Carlowttz), Warasdin, and Hanoi
Generalnie : the Liccu Regiment (headquarters at Gospic)t), the Otto-
cliaz Iteginient (Ottochaz), the Ogulin (Ogulin), the Sluin (Carlstadt),
tlie Cross (Belovar), the St Geoi-ge's (Belovar), the 1st Banal (Glina),
the 2d Banal (Petrinia). (2) Tlie Slavonian Otneralale: the Gradiska
Regiment (Neu Giadiska), the Brood Regiment (Vinkoveze), the Peter-
wardein (llitrovicz), the Tcli.iikist BatUlion (Titel). (3J The Hanoi
O'oieralale : the German Banat Regiment (Pancsova), the Wallachiatt
Banat (Karansebes), the Illjrian Banat (Weisskirchen). (4) 7/« Tran-
sjhaiiian Genemlule: The Szekler Regiment No. 14 (Csik Szered«)w
the Szekler Regiment No. 16 (Keszdi Vasarbely), the WaUachian NoJ
16 (Orlath), the WaUachian No. 17 (Naszo-l). Twelve towns, knowJ
as "military communities" had communal constitutions not unlike
those of the free towns of Hungary— Car iopago, Zengg, Petrinia, Kon-
tJiiuicza, Belovar, Ivauif, BroOj^ P£terw»rdein, CarbwiU.^Semli*^
Paacaova, and Weiaskirrhpn.
296
MILITARY LAW
IVnops were raised for a partienlar serrice, and were dis-
banded uion the cessation of hostilitif^ The cromi, of its
mere prerogative, made laws known as Articles of War,
for the government and discipline of tbe troops while thun
eml)odie<.l and serving. Except for the punishment of
desertion, which offence was made a felony by statute in
the reign of Henry VI., the."!e ordinances or Articles of
ViHT remained almost the sole authority for the enforce-
tcent of discipline until 1C89, when the first Mutiny Act
was pas.>ied and the military forces of the crown were
brought under the direct control of parliament. Even the
Parliamentary forces in the time of Charles I. and Cromwell
were governed, not by an Act of the Icgi.'ilature, but by
articles of war similar to those issued by the king and
authorized by an ordinance of the Lords and Commons,
exercising in that respect the sovereign prerogative. This
jxjwer of law-making by prerogative was, however, held to
be applicable during a state of actual war only, and
attempts to exercise it in time of peace were ineffectual.
Subject to this limitation it existed for considerably more
than a century after the passing of the first Mutiny Act.
From 1G89 to 1803, although in peace time the Mutiny
Act was occasionally suffered to expire, a statutory [tower
was given to the crown to make Articles of War to operate
in the colonies and elsewhere beyond the seas in the same
manner as those made by prerogative operated in time of
war. In 17 lo, in consequence of the rebellion, this power
was created in respect of the forces in the kingdom. But
these enactments were apart from and in no respect affected
the principle acknowledged all this time that the crown of
its mere prerogative could make laws for the government
of the army in foreign countries in time of war. The
Mutiny Act of 180.3 effected a great constitutional change
in this respect : the power of the crown to make any
Articles of War became altogether statutory, and the pre-
rogative merged iu the Act of Parliament. So matters
remained till the year 1879, when the last Mutiny Act
was passed and the last Articles of War were promulgated.
The Mutiny Act legislated for offences in respect of which
death or penal servitude could be awarded, and the
Articles of War, while repeating those provisions of the
Act, constituted thq dii-ect authority for dealing with
offences for which imprisonment was the maximum punish-
ment as well as with many matters relating to trial and
procedure. The Act and the Articles were found not to
liannonize in all respects. Their general arrangement was
faulty, and their language sometimes obscure. In 18G9 a
royal commission recommended that both should be recast
iu a .simple and intelligible shajK;. Iu 1878 a committee
of the House of Commons endorsed this view and made
certain recommendations as to the way iu which the task
should be performed. In 1870 the Government submitted
to parliament and passed into law a measure consolidating
in one Act both the Mutiny Act and the Articles of War,
and amending their provisions in certain important respects.
This measure was called the "Army Discipline and
Regulation Act, 1879." After one or two years' exiierience
of its working it also was found capable of improvement,
and was in it.s turn superseded by the Army Act, 1881,
which now forms the foundation and the main portion
of the military law of England. It contains a proviso
saving the right of the crown to make Articles of War,
but in such a manner as to render the power in effect
a nullity ; for it enacts that no crime made punishable by
the Act shall be otherwise inmishable by such Articles.
As the punishment of every conccivalile offence is provided
for by the Act, any Articles made thereunder can be no
more than an empty formality having no practical effect.
Thus the history of English military law up to 1879 may
be divided into three periods, each having a diatinct con-
stitutional a3i>cct : — (1) that prior to 1G89, when the army,
being regarded as so many personal retainers of the
sovereign rather than servants of the state, was mainly
governed by the will of the sovereign ; (2) that between
1689 and 1803, when the army, being recognized as a. per-
manent force, was governed within the realm by statute
and without it by the prerogative of the crown ; and (3)
that from 1803 to 1879, when it was governed either
directly by statute or by the sovereign under an authority
derived from and defined and limited by statute. Although
in 1879 the power of making Articles of War became in
effect altogether inoperative, the sovereign was empowered
to make rules of procedure, having the force of law, which
regulate the administration of the Act in many matters
formerly dealt with by the Articles of War. These rules,
however, must not be inconsistent with the provisions of
the Army Act itself, and must be laid before parliaaueut
immediately after they are made. Thus in 1879 the
government and discipline of the army became for the first
time completely subject either to the direct action or the
close supervision of parliament.
A further notable change took place at the same time.
The JIutiny Act had been brought into force on each
occasion for one year only, in compliance with the con-
stitutional theory that the maintenance of a standing army
in time of peace, unless with the consent of parliament, is
against law. Each session therefore the text of the Act
had to be passed through both Houses clause by clause and
line by line. The Army Act, on the other hand, is a fixed
permanent code. But constitutional traditions are fully
respected by the in.sertion in it of a section providing that
it shall come into force only by virtue of an annual Act of
Parliament. This annual Act recites the illegality of a
standing army in time of peace unless with the consent of
parliament, and the necessity nevertheless of maintaining a
certain number of laud forces (exclusive of those serving
in India) and a body of royal marine forces on shore, and
of keeping them in exact discipline, and it brings into force
the Army Act for one year.
Military law is thus chiefly to be found in the Army Act
and the rules of procedure made thereunder, the Militia Act,
1882, the Reserve Forces Act, 18S2, and the Volunteer
Act, 18r.3, together with certain Acts relating to the
yeomanry, and various royal warrants and regulations.
The Army Act itself i-s however, the chief authority.
Although the comi'laint has l>een sometimes made, and not
without a certain amount of reason, that it docs not accom-
plish much that it might in i>oint of brevity, simplicity,
and clearness of expression, it is a very comprehensive
piece of legislation, and shows some distinct improvements
upon the old Mutiny Acts and Articles of War.
The persons subject to military law are the officers oa
the active list and the soldiers nf tlie regular forces (includ-
ing the royal marines), the i>ermancnt staff of the auxiliary
(i.e., the militia, volunteer, and yeomanry) forces, and the
officers of the militia. The above persons are amenable to
its provisions at all times except while embarked on board
a commissioned ship of the royal navy, when they becoma
subject to the Xaval Disci[iline Act and certain orders id
council made under its authority. Tho>e who are subject to
military law in certain circumstances only arc^-officcrs and
men while serving in a force raised out of the United
Kingdom and commanded by an officer of the regular
forces ; jKusioners when employed in military service
under the command of a regular officer ; the non-conmiis-
sioned officers and men of the militia, during training,
when attached to the regulars or when jiermanently
cmlxxlied ; the officers rtf the yeomanry and the volunteer*
when in corJiuand of or attached to a body of men Mubject
to militflrj' law, or when their corp» is on-Mtual military
MILITARY LAW
297
seraea, ot when ordered on duty with their own consent ;
the men of the yeomanry when they or their corps are being
(rainedj when they are attached to or acting with the
regular forces, when their corps is on actual military service,
or when serving in aid 'of the civil power ; the men of the
volunteers when they are being trained with or are attached
to any body of troops, or when their corps is on actual
military service ; the men of the army reserve and the
militia reserve when called out for training or on duty in
(Ltd of the civil power ; any ' person who in an official
capacity equiv^ent to that of an officer accompanies a
body of troops on active service beyond the seas; any
person accompanying a force on active service holding a
pass from the general entitling him to be treated on the
footing of an officer. In this last category would of course
be included newspaper correspondents, also sutlers and
followers. In one or two cases persons are subjected
to military law to a limited extent and in respect only of
certain offences. Thus a militiaman even when not out
ffor training or not embodied is liable to a military trial
and punishment for fraudulent enlistment or making a
false answer on attestation. In the same meuiner an army
reserve man may be tried and punished by court martial
for neglect to appear at the place where he is bound
periodically to report himself, or for insubordination to his
superiors on these occasions, or for any fraud in connexion
with the receipt of his pay. A man of the army reserve
6r the militia reserve has the legal status of and in fact
becomes a regular soldier when called out on occasions of
national danger or emergency under the sovereign's pro-
plamatioqL
When a person subject to military law commits an
offence he is taken into military custody, which means
either arrest in his own quarters or confinement. He
must without unnecessary delay be brought before his
commanding officer, who upon investigating the case may
dismiss the charge if in his discretion he thinks it ought
not to be proceeded with, or may take steps to bring the
offender before a court martial Where the offender is not
au officer he may dispose of the case summarily, the limit
of his power in this respect being seven days' imprison-
ment with hard labour, fines not exceeding 10s. for
drunkenness, certain deductions from pay, confinement to
barracks for twenty-eight days, this involWng severe extra
drills, deprivations, and other minor punishments. Where
the offence is absence without leave for a period exceeding
seven days, the commanding officer may award a day's
imprisonment in respect of each day of such absence up
to twenty-one. It is only in the case of the imprisonment
exceeding seven days that the evidence before the com-
manding officer is taken on oath, and then only in the
event of the accused so desiring it. The commanding
officer is enjoined by regulation not to punish summarily
the more serious kind of offences, but his legal jurisdiction
in this respect is without limit as regards any soldier
brought before him, and when he has dealt summarily
with a case the accused is free from any other liability in
respect of the offence thus disposed of. In any instance
where the commanding officer has summarily awarded
imprisonment, fine, or deduction from pay, the accused
may claim a district court martial instead of submitting
to the award.
Ordinary courts martial are of tnree kinds, viz.: — (I) a
regimental court martial, usually convened and confirmed
by the commanding officer of the regiment or detachment,
presided over by an officer not under the rank of captain,
oomposed of at least three officers of the regiment or
detachment with not less than one year's service, and
Ikaving a maximum power of punishment of forty-two days'
imprisonment with hard labour ; (2) a district cjurt
martial, usually convened by the general of the district,
consisting in the United Kingdom, India, Malta, and
Gibraltar of not less than five and elsewhere of not less
than three officers, each with two years' service or more,
and having a maximum power of punishment of two years'
imprisonment with hard labour ; (3) a general court martial,
the only tribunal having authority to try a commissioned
officer, and with a power of punishment extending to death
or penal servitude, for offences for which these penalties
are authorized by statute; it consists of not less than
nine officers in the United Kingdom, India, Malta, and
Gibraltar and of five elsewhere, each of whom must have
over three years' service, five being not vmder the rank of
captain. There is another kind of tribunal incidental to
service in the field, or where, in the case of an offence
against -the person or property of an inhabitant, an ordinary
court martial cannot be held, namely, a field general court
martial This court may consist of three officers only, and
it has the power of sentencing to death. Another kind of
court, called a summary court martial, may be held where
an offence has been committed upon active service and an
ordinary court cannot be conveniently assembled. In the
event of three officers not being available it may consist of
two. When thus constituted it can award only a "summary
punishment" or imprisonment; where it consists of three
officers, however, it can sentence to death. In the case ol
a field general or a summary court martial many forma
and precautions prescribed in the case of ordinary courts
are not necessarily observed, the whole proceeding being
from the necessity of the case a somewhat rough and ready
means of dealing promptly with crime.
The Army Act prescribes the maximum )iunishment which raaj
be inflicted in respect of each offence. That of death is incurred
by various acts of treachery or cowardice before the enemy, or by
when on active service interfering with or impeding authority, leav-
ing without orders a guard or post, or when sentry sleeping or being
drunk on a post, plundering or committing an offence against tlM
person or property of an inhabitant, intentionally causing fala*
alarms, or deserting. Whether upon active service or not, a soldier
also becomes liable to the punishment of death who mutinies or ii>-
cites to or joins in or connives at a mutiny, who uses or offers violence
to or defiantly disobeys tlie lawful command of his superior officv
when in the execution of his office. Penal servitude is the maximum
punishment for various acts and irregularities upon active scrvioo
not distinctly of a treacherous or wilfully injurious character, for
using or offering violence or insubordinate language to a su]ierior, or
disobeying a lawful command when upon active service. The same
punishment is applicable when not upon active service to a second
offence of desertion or fraudulent enlistment (i.e., enlistment by
one who already belongs to the service), certain embezzlements of
public property, wilfully releasing without authority a prisoner or
wilfully permitting a prisoner to escape, enlisting when previously
discharged from the sei-vice with disgrace without disclosing the
circumstances of such discharge, or any other offence which by the
ordinary criminal law of England is punishable with penal ser-
vitude. Imprisonment with hard labour for two years is the
maximum punishment for minor forms and degrees of those offencee
which if committed upon active service would involve death or
penal servitude, such as using or offering violence or insubordinate
language to a superior or disobeying a lawful command, and for the
following offences: — resisting an escoit, breaking out of barmcka,
neglect of orders, a first offence of desertion or attempted desertion
or aiding or conniviug at desertion, or of fraudulent enlistment,
absence without leave, failure to appear at parade, going beyond
prescribed bounds, absence from school, malingering or produc-
ing disease or infirmity, maiming with intent to render a soldier
unfit for service, an act of a fraudulent nature, disgraceful con-
duct of a cruel, indecent, or unnatural kind, drunkenness, releasing a
prisoner without proper authority or allowing him to escape, bt-ing
concerned in the unreasonable detention of a person awaiting trial,
escaping or attempting to escape from lawful custody, conniving at
exoroitant exactions, making away with, losing by neglect, or wilfully
injuring military clothiug or equipments, ill-treating a horse useJ
in the serrice, making false or fraudulent representations in public
documents, making a wilfully false accusation against an officer ot
soldier, making a false confession of deserMon or fraudulent enlist*
ment, or a false statement in respect of the prolongation of furloe^h.
misconduct as a witness before a court martial or contempt of eueli
court, giving false evidence ou oath, any offence specified in reiatieo
XVL — »8
293
Ma L I.T A R Y LAW
to billeting or the impressment of carriages, making a false answer
to a question pnt upon attestation, being concerned in unlawful
enliBtment, using traitorous or disloyal words regarding the
BJTereign, disclosing any circumstance relating to the numbers,
|)oeition, movements, or other circumstances of any part of her
jnajesty's forces so as to produce effects injurious to her majesty's
service, fighting or being concerned in or conniving at a duel,
attempting suicide, obstructing the civil outhoiilies in the apprehen-
sion of any officer or soldier accused of an offence, any conduct,
disorder, or neglect to the prejudice of good order aud military dis-
cipline, any offence which if committed in Englaud would I* puuisli-
able by the law of EnglauiL There is another offence which can be
committed by officers only, namely, " scandalous conduct unbecom-
ing the character of an officer aiid a gentleman." It necessitates
cashiering, a punishment which in the case of an officer may be
awarded as an alternative to imprisounicnt in several other instances.
There is also an offence peculiar to officers and nou-conimissioned
officers, that of striking or ill-treating a soldier or unlawfully
detaining his pay. A sentence of ciLsIiiering as distinguished from
that of dismissal in the case of an officer involves an incapacity to
serve the crown again. An officer may be also sentenced to forfeiture
of seniority of rank and to reprimand or severe rc-primand. A
non-commissioned officer may bo sentenced to be reduced to a lower
grade or to the rauks, and where sentenced to pen;d servitude or
imprisonment is deemed to be reduced to the ranks. The com-
mander-in-chief at home or the commander-in-chief in India or in
either of the presidencies may also cause a non-commissioned officer
to be reduced to a lower gi-ade or to the ranks. An acting non-
commissioned officer may be ordered by his- commanding officer for
an offencs or for inefficiency or otherwise to revert to his per-
manent grude, — in other words, to forfeit his acting rank-
It will have been observed that persons subject to military law
are liable to be tried by court martial for offences which if com-
mitted in England would be punishable by the ordinary law, and to
suffer either the punishment prescribed by the ordinary criminal
law or that authorized for soldiera who commit offences to the
f)rejudice of good order and military discipline. The effect of the
alter alternative is that for many minor offences for whicli a civilian
is liable to a short term of imprisonment, or perhaps only to a fine,
a soldier may be awarded two years' imprisonment with hard labour.
A court martial, however, cannot take cognizance of tlie crimes of
treason, murder, manslaughter, treason-feloiiA', or rape if committed
in the United KingdouL If one of these offences be committed in
any place within her majesty's dominions other than the United
Kingdom or Gilw-altar, a court martial can deal with it only if it be
committed on active service or in a place more than 100 miles fronr
a civil court having jurisdiction to try the offence. With regard to
all civil offences th© military law, it is to bo understood, is subor-
dinate to the ordinary Jpw, and a civilian aggrieved by a soldier
in respect of a criminal offence against his property or person
does not forfeit his right to prosecute the soldier as if he were a
civilian.
Xhe crimes for which soldiers are most usually tried are desertion,
absence without leave, loss of necessaries, violence or insuboi-dina-
tion to superiors, drunkenness, and various forms of conduct to the
prejudice of disci|iline. The punishments are generally speaking
gauged as mucli with regard to the character and antecedents of
the prisoner as to the particular offence. For a first offence of an
ordinary kind a district court martial would give as a rule fifty-six
days' imprisonment with hard labour, for a second or graver crime
eighty-four days. There are not many instances in which the
period of imprisonment exceeds six months. Corporal punishment,
which had been practically limited to offences committed upon
active service, and in 1879 to crimes punishable with death, was
finally abolished in 1881, and a summary punishment substituted.
This siHnmary punishment includes the liability for a term of three
months to be kept in iron- fetters and handcuffs, aud while so kept
to bo attached to a fixed object so that the offender may remain in
a fixed position for a period not exceeding two hours in the day for
not more than three out of any four consecutive days and for not
more than twenty-one days in the aggregate. The offender may
also be subjected to the like labour and restraint, and may be dealt
iwith in the samo nmnner as if sentenced to hard-labour imnrison-
raenL But th(?fti) summary inmishments ore to be inflicted so as
not to cau<;e injnry to healtti or leave a nermanent mark on the
offender. Tlie firet instances in which tliis kind of punisliment
,wa3 inflicted occurred during the campaign of 1882 in Egypt
Estimated by the results, the abolition of flogging does not apjiear
^o have injuriously affected discipline, the conduct of the troops in
Egypt having been exceptionally good. The jiractice of marking a
soldier with the letters *'D" (deserter) or "llC" (bad character).
in order to prevent his re-enlistment, was abolished about a dozen
years ago in d<.'fcicnce to public opinion, which erroneously adopted
the idea thut, ih-i "markmg" was effected by red-hot irons or in
some other manner involving torture Military men for the moat
part regret iU abolition, and maintain that if tlic practice were still
in force the army would not be taiutcd by the presence of many bdd
characters who finu means of eluding the vigilance of the authorities
and enlisting after pi-evioas discharge.
The course of procedure in military tiials ia as follows. 'When a.
soldier is remanded by his commanding officer for trial by a district
or general court martial, a copy of the charge, together witU tho
statements of the witnesses for the prosecution (called the sum-
mary of evidence), is furnished to him, and lie is given piopir opi>or-
tunity of preparing his defence, of communicating with his witnesses
or legal adviser, aud of procuring the attendance of his witnesses.
Further, if he desires it, a list of the officers appointed to form the
court shall be given him. Any officer is disqualified to hit as a
member who has convened the court, wlio is the prosecutor or a
witness for the prosecution, who has made the prchniinary injury
into the facts, who is the prisoner's commanding officer, or who has
a pei-sonal interest in the case. The prisoner may also object to
any officer on the ground of bias or prejudice similarly as a ciriliau
might challenge a juror. Except as regards the delay caused by
tho writing out of the evidence, the procedure at a court martial
is very much the same as that at an ordinary criminal trial,— the
examination and cross-examination of the witnesses, addresses of tho
prosecutor and prisoner, aud the rules governing the admission or
rejection of evidence being nearly identical. At a general court
martial, and sometimes at a district court, a Judge advocate repre-
senting the judge advocate general officiates, his functions being very
much those of a legal assessor to the court He advises upon all points
of law, and sums up the evidence just as a judge charges a jury.
When the prisoner jileads guilty the court fimls a verdict accord-
ingly, reads the summary of evidence, hears any statement in
mitigation of punishment, aud takes evidence as to character before
proceeding to pass sentence. The sentence is that of the majority
of the court, except where death is awarded, when two-thirds of tho
members in the case of a general court martial and the whole iu
that of a field general court martial must concur. When an ac'iuitUd
upon all the charges takes place the verdict is announced in open
court, and the prisoner is released without any further proceeding.
When the finding is "guilty," evidence as to character is takeL,
and the court deliberates in private upon the sentence, but the
result is not made known until the proceedings are eonfimied and
promulgated. No conviction or sentence lias any effect untU it is
thus confirmed by the proper authority. The confinning authority
in the case of a regimental court is the comniauding officer, in that
of a district court martial the general officer commnndine. the
district, and in that of a general court, if held, in the United
Kingdom her majesty, and if abroad in most cases the general officer
commanding. The c^anfirftiing authority may order the reaiscnibling
of the court in order that an J question or irregularity may be revised
and corrected, but not for the purpose of increasing a sentence. He
may, however, of his own discretion, and without further reference
to the court, refuse confirmation to the whole or any portion of tha
finding or sentence, and he may mitigate, commute, or entirely
remit the punishment In thj case of a general court martial
the proceedings are sent to the judge advocate general, who submits
to the queen his opinion as to the legality of the trial and sentence.
If they are legal m all respects he sends the proceedings to the
commander-in-chief, upon whom rests the duty of advising the queea
regarding the exercise of clemency. In addition to confirmation,'
however, every general or district court martial held out of India
lias another ordeal to go through. It is reviewed and examined in
the office of tlu judge advocate general, and any illegality that may
be disclosed is corrected and the prisoner is relieved of the con-
sequences. To a lertaiu extent a protection against illegality also
exists in thecase of regimental courts martial. A mon4lily return
of those held in each regiment is laid before the general command-
ing the district or brigade, by whom any question that might appear
to him doubtful would be referred to the adjutant genei-al or tU«*
^udge advocate general for decision. It is to be noted, liowever, that
the judge advocate gsneral, although fulfilling duties which arc in
their nature judicial, is only an adviser. He is not actually a judge
in an executive sense, and has no authority directly to interfere with
or correct an illegal conviction. In many cases the law thus pro-
vides no rt- mcdy lor an officer or soldier who may have been wronged
by the finding or sentence of a court martial, — for instance,'
through a verdict not justified by tho evidence or through a non-
observance of tho rules aud practice prescribed for these tribunalB.1
A person who has suffered injustice may appeal to the Queen's Uencli'
division of the high court of justice. But, speaking gencrnlly, that
tribunal would not interfere with a court martial exercising its
jurisdiction within the law as regards the prisoner, the crime, and
tho sentence. In most cases, therefore, tho virtu.il protector of nn
accused |>crson against illegality is the judge advocate gentM-al,
who personally advises the queen and the military antlioritics that
tho law shall be complied with. As a privy councillor and member
of the House of Commons that oflicor is lebitonsiblo \>o\}\ to the'
queen and to parliament for the right and due aJmiuistiation of
military law; and. notwithstinding his want of direct cxecuiivo
authority, it is not to be contemplated that any inilii.iiy ofliWr
would hesitate to art upon advice given by hiiB with rcfiicius to a
M I-L — M I L
299
Ifg!>l qncstion conTiectol with a conrt nmrtial. The department of
the judge advocate general consists of the judge advocntc peneral,
who is a lawyer, a privy councillor, and a member of parliament,
of a permanent deputy judge advocate general who is also a lawyer,
and of three military officers as deputy judge advocates having
special experience in the working of military law.
The Army Act applies to European officers and soldiers serving in
India in the same manner as to the rest of the army, but natives
of India are governed by their own Articles of War, and in the case
of civil oflTences they are dealt with according to the provisions of
the Indian penal code. The department of the judge advocate
general in India is distinct from and independent of that of the
judge advocate general of the army, and courts martial held in that
country are not subject to the supervision of a profe^jsional Iaw}*er.
Certain prominent irregularities led to the appointment of a
barrister as judge advocate general in India in 1869, but after a few
years that appointment again became filled by a military officer.
The staff of the department is, however, far more nnmerous in India
than elsewhere. There are judge advocates general for each of
the presidencies, and a deputy judge advocate at each of the more
impoitant military centres.
Statistics of Crime in the .^rnii/. —Commissioned officers are
rarely subjected to trial by court martial. Where an officer com-
mits himself in a military sense, and his misconduct is too serious
to be passed over merely with a mark of official displeasure, he is
nsually given and seldom fails to accept the alternative of resigning
his commission. In some instances the crown is advised to exercise
Its prerogative and remove him from the army on the ground that
her majesty has no further occasion for his services. In no c -cum-
stances can an officer or soldier claim a court martial as a right
In tha result, the annual number of trials of officers does not average
more than four of late years. Amon" the non-commissioned officers
and soldiera of the army, however, the trials and summary punish-
ments by commanding officers are exceedingly numerous, as will
presently be seen. In India this observation hardly holds good, for
ID that country desertion is physically almost impossible except at
the two or three seaports where troops are stationed. Absence
without leave is for a similar reason ol^ rare occurrence, while the
*• . .^f 41. i ,. • . it ■ 4.1.1V, Mionuv-titc icitbuicui tut^ rrcDcu system is 1
ftict of the troops living in their own cantonments, and Deing free of regiments of discipline for refracto.7 characters.
from many temntations of life existing in the large towns and garri- general officer's power of imprisonment (two months
sons at home, places them outside the influence of certain prevalent the olTender may be sent before a court of di-;cipline '
causes of crime. For this reason mainly the proportion'of
martial held in 1881 was 107 per 1000 men at home as compared
with 76 abroad. Similarly the proportion of minor punishments
per 1000 was 1449 at home to 1042 abroad It is also generally
found that men engaged upon active service in th? field commit
less crime than those serving in ordinary circumstances. But the
general criminal statistics of the army for 1881 show a formidable
amount of crime and punishment. Upon an average strength of
131,186 non-commissioned officers and men there were 16,523 courts
icartial, of which 179 were general, 8549 district, and 7796 regi-
mental courts. There were also 224,681 minor punishments by com-
manding officers, including 44,108 fines for drunkenness. These
figures generally show an increase of crime as compared with the
two years immediately preceding, but these two exhibited a decrease
npon previous years. Of the offences tried by court martial in
1881 the following were the principal:— mutiny 7, desertion 1597,
offences in relation to enlistment (fraudulently enlisting while
already belonging to the service or making false answers npon
attestation) 1190, violence to and disobedience of superiors 1650,
minor insubordination and neglect of orders 1472, quitting or sleep-
ing on post 681, drankenness on duty 266], drunkenness (tried by
court martial when the offence has been committed on a fifth
occasion within twelve months) 2147, disgi-oceful conduct of various
kinds 660, absence without leave not amounting to desertion 3293,
makiug away with or losing by neglect equipment or necessaries
S768, and miscellaneous offences chiefly of an ordinary criminal
character or to the prejudice of discipline 4181. Upon the 16,523
trials there were 349 findings of acquittal Regarding the punish-
ments awarded, it appears that no soldier was sentenced to death
during the year, and the otlier awards were as follows :— penal
•ervituda 104, imprisonmeot with or without hard labour (alinost
Invariably the former) 12,125, discharge with ignominy without
other punishment 42, stoppages of pay without other piinishment
65, flogging (before the abolition of that punishment by the Act of
1881) 16, and the new summary punishment (authorized as a sub-
stitute for flocging) 3. Of the non-commissioned officers 3228
.Tore punished by reduction to a lower giade or to the ranks, while
691 more suffered imprisonment in addition to loss of grade, the
former number being in the proportion of about 12 and the latter
of 2 per cent to strength. Of the men tiied 305 were pardoned.
Militan/ Law 0/ other Counlria.— The administration of military
l«w in other countries having large armies harmonizes in many
important respects with that of England. In some indeed it is a
question whether their systems are not superior and in advance.
They hav» a considerable boily of " auditors " or military lawyers
who expouud'the law and do much to secure a uniTotm uid exact
administration of justice. Thns In Austria there are nhont five
hundred of these auditors, one being attached to each regiment. In
the same' country there are also courts of appeal from the courts of
first instance, these latter consisting of eight persons including ths
auditor. Where the prisoner is a non-commissioned officer or a
private, that rank is represented on the court. Here also the
confirmation of superior authority is required. In the German
army there are general and regimental courts. An auditor who
is a lawyer is attached to each division, and it is his duty to
expound the law, collect the eridence, and read it to the court
in the presence of the prisoner, who is asked if he has any thing to
say. The court consists of eleven members, of whom upon the trial
of a private soldier or non-commissioned officer three are of the
rank of the accused. The power of commanding officers in regard
to disciplinary nunishments is greater than in the British anny,
especially in relation to officers, who may be placed in arrest for
fourteen days. The non-commissioned officers and privates are liable
to extra guards, drills, fatigues, and different degrees of arrest, some
of a very severe character. Dismissal from the army, which is r».
garded as a most severe punishment, invoh-ing civil disgrace,
often awarded. In Russia there are three kinds of military courts-
naniely, the rerimental court martial, the tribunals of military
districts, and the supreme tribunal at St Petersburg. They art
permanent courts, are attended by legal persons, and in certain
instances have jurisdiction over the civil population as well as the
army. There is a judge advocate general at St Petersburg, where
the supreme tribunal consists of general officers and high war-office
functionaries who have studied military law or possess a largt
experience of its working. In Italy there are permanent njilitar
tribunals for the tiial of non-commissioned omcei-s and soldier;
while special tribunals are appointed to try officers. The court is
the absolute judge of the facts, but regarding legal errors or
irregularities an appeal lies to the supreme war tribunal, which con-
sists of four civilian judges and three general officers. The French
code corresponds in many resDdts with those of the other great
Continental armies, but it tends rather to give individual officers
large powers of imprisonment graduated according to their rank.
The chief disrinctive feature of the French system is the institution
When th.
ths) is exhausted
may be sent before a conrt of discipline and by them
drafted into a covtpngnie de discipKiu ; and cases of habitual miscon-
duct are thus dealt with, the man being struck off the strength of
his original corps and transferred to one in Algeria. The military
law of the United States is founded upon and proceeds much niior
the same lines as that of England. (J. c O'D )
MILITAKY TACTICS. See Wae.
MILITIA. Tlio militia of the United Kingdom
consists of a number of officers and men maintained for
the purpose of augmenting the military strength of the
country in case of imminent national danger or great
emergency. In such a contingency the whole or any pari
of the militia is liable, by proclamation of the sovereign,
to be embodied, — that is to say, placed on active military
service within the confines of the United Kingdom. The
occasion for issuing the proclamation must be first com
municated by message to parliament if it be then in session;
if it be not sitting, parliament must be called togethei
within ten days. For the purpose of keeping the force in
a condition of military efficiency, the officers and men are
subjected to one preliminary training for a period not
exceeding six (usually about two) months, and further to
an annual training not exceeding fifty-six (usually twenty-
eight) days. The force is composed of corps of artillery,
engineers, and infantry. Infantry militiamen are formed
into battalions constituting part of the territorial regiment
of the locality of which the regular forces are the senior
battalions. The officers and men when called out are Lable
to duty with the regulars and in all respects as regular
soldiers within the United Kingdom. Of late years the
men have been raised exclusively by voluntary enlistment,
but where a sufficient number for any county or place is not
thus raised a ballot may be resorted to in order to complete
the quota fixed by the queen in council for that county or
place. Each man is enlisted as a militiaman for the couoty,
to serve in the territorial regiment or corps of the dist 'ict.
The period of engagement is not to exceed six years, but
during the last of these years 'a militiaman may be re-
engaged for a further period also not exceeding six ye rs.
300
MILITIA
Mbn who illegally absent themselves are liable, in addition
to punishment for the offence, to make up for the time of
their absence by a corresponding extension of their service.
The officers are appointed and promoted by the crown, but
first appointments are given to persons recommended by
the lord lieutenant of the county who may be approved
a-s fulfiliing the prescribed conditions in respect of age,
physical fitness, and educational qualifications. Since 1877
the officers have been permanently subject to military law.
The general body of the non-commissioned officers and men
are so subject only when called out for training or embodi-
ment. At other periods they have simply the legal status
of civilians, except as regards a liability to trial and
punishment for offences in connexion with enlistment or
for military offences committed while called out. Each
militia regiment has a permanent staff, consisting of an
li^jntant and a small body of non-commissioned officers and
drummers, to conduct the recruj|ing drills and ordinary
business of the corps; and the members of this permanent
staff are always subject to military law. They mostly
consist of non-commissioned officers who belong to or
have served La the regular portion of the territorial
regiment. Many of the militia corps have their head-
quarters at the brigade dep6t or local establishment of the
territorial regiment, and all are under the general supervision
of the (regular) colonel commanding the brigade dep6t.
The area of service does not extend beyond the United
Kingdom ; but those who voluntarily offer to serve in the
Channel Islands, the Isle of Man, Malta, or Gibraltar may
be employed therein. The uniform of the officers and men
of the militia is precisely the same as that of the regular
ci»ps with which they are associated, or rather of which
Ifcey form part, except that in addition to the regimental
distinguishing mark they bear the letter " M " upon their
appointments, to denote that they belong to the militia
portion of the corps.
A a above stated, the ranks of the militia are usually
filled by voluntary enlistment; but by a statute which,
though temporarily suspended, can be put in force provi-
sions are made for filling up any deficiency in the allotted
quota in any county, city, or riding by ballot ef the male
inhabitants if ivithin certain limits of age. The enactment
pi-ovides as follows: —
The secretary of state is to declare the number of militiamen re-
quired, whereupon the lord lieutenant 13 to cause raeetiuf^ to be
held of the lieutenancy for each subdivision. To these meetings the
householders of each parish are to send in lists of all male persons
between the ages of eighteen and thirty dwelling in their respective
houses. Before the ballot, however, the parish may supply volun-
teers to fill up the quota, every volunteer so provided and approved
counting as if he were a balloted person. If a deficiency still
exists, the persons on the lists shall bo balloted for, and double the
number of those required to supply tlie deficiency shall be drawn
out Any person whose name is so drawn may chum exemption or
object; and the deputy lieutenants settle the question of hia liability
to serve. From trie corrected list those who are of the requisite
physique (the height is 6 feet 2) are enrolled in the order in which
their names are numbered until the quota is completed. If the list
is not sulhcieut to fill the quota, another ballot iu the same manner
is to bo t;iken. Any balloted man becoming liable to serve may,
however, provide a substitute who has the requisite physical qualiii-
tiations, and is not himself liable to serve.
Within the general body of the militia is contained
another having an additional and important obligation in
the matter of service. It is called the "militia resor\'o,"
and is formed of men who voluntarily undertake a liability
to join the regular forces and servo in any place to which
they may be ordered in case of the proclamation of a state
of imminent national danger or great emergency. In this
respect they are in fact upon the same footing as the army
reserve, and on the occasion of the mobilization of 1878
more than 20,000 of these men became part of the regular
army. The present strength of the militia reserve is a
little under 29,000 men, and judging by past experience it
may be computed that about i!5,000 coiUd bo at once
added to the ranks of an army in the field in the event of
national danger or emergency. It is to be observed, hoT»^1
ever, that every man thus added to the regulars would be
taken away from the effective strength of the militia, ^
There is no statutory provision for the number of meo'
to be maintained, that number being what from time to
time may be voted by parliament. Tlie latest information
available respecting the actual condition of the militia of
Great Britain relates to the year 1881, and that of Ireland
to 1880, the militia of the latter country for obvious
political reasons not having been called out for training in
1881 or 1882. Taking the militia of the United Kingdom
in 1881, we find that the establishment provided for was
139,501, of whom 18,618 were artillery, 1317 engineers,
and 1-19,566 infantry. Divided into ranks, this establish-
ment was made up of 3534 sergeants and 12G0 drummers of
the permanent staff, and of the general body 3909 officers,
2520 sergeants, 5040 cor;)orals, and 123,238 privates.
The number actually enrolled was 127,868 of all ranks,
leaving 11,633 wanting to complete. Of the number
enrolled 84,864 belonged to English, 14,138 to Scotch, and
28,866 to Irish regiments, the numbers wanting to complete
being for England 7420, for Scotland 162, and for Ireland
4051. As the Irish regiments were not called out, our
information regarding the actual effective condition of the
force as shown at the annual training does not include
Ireland. With regard to the English regiments, 74,946
were present out of an enrolled strength of 84,864. Of
the absentees 3144 were with and 6775 without leave.
In the Scotch regiments, 12,401 appeared at the training,
and of the absentees 616 were with leave and 1121 mib.-
out. Of the total estabUshment (106,584) for Great
Britain, 99,002 were enrolled, and of those enrolled 87,348
presented themselves and 3760 were absent with leave and
7896 actual defaulters. Of the English regiments five-
sixths and of the Scotch regiments two-thirds were bom in
the county to which their regiments respectively belonged.
Of 92,677 men (for Great Britain) whose occ-pationi
are disclosed, 17,665 were artisans, 22,221 mechanicfl
labourers, 26,227 agricultural labourers, and 26,564 other
trades. Speaking approximately, more than one-half of
the men were between twenty and thirty years of age,
about 4 per cen.. between seventeen and eighteen, about
9 per cent, between eighteen and nineteen, and about 12
per cent, between nineteen and twenty, while some 20 per
cent, were over thirty years of age. More than one-half
those inspected in 1881 were between 5 feet 5 inches and
5 feet 7 inches in height, about 20 per cent. were, under 5
feet 5 inches, while only 585 out of a total of 92,677 were
6 feet and upwards. At the date of inspection there were
296 men in military confinement and 465 in the custody
of the civil power. On the last occasion (18S0) on which
the Irish militia were called out, upon an establishment
of 32,813 and an enrolled strength of 30,515 the number
present at the training was 26,399, leaving 706 absent -with
and 2264 without leave. Regiments numbering in the
aggregate 1146 men were not trained.
As distinguished from the regular forces or standing array, the
militia has been described as the constitutional military force of tha
country ; and its history justifies the description, at least up to »
recent period when it lost its distinctive character and became to s
great extent merged in the regular army. It is the oldest force
firilaiu possesses, and in fact represents the train bands of early
English history. Its origin is to be found in Iho obligation of all
freemen between certain ages to arm themselves for the preservation
of tho peace within tlieir respective counties, and genomlly for the
protection of tho kingdom from invasion. This obligation, inipoaed
in tho fii-bt in»t.inee upon tho individuals themselves, became shifted
to tlio owners of land, who were com|)elled to keep up their proper-
tion of hor-.ea and armour for tho national defence. The force* wee*
M I L — M I L
rem^ained 4 near i centSr^ wUh th"'^ *''° f '"^ "f England
community. It was recom^Jn T '■''^ K'^"""' approval of the
for the pr;«rvatTon of !^ "1? "^ 'nstrument for defence and
popular Fromihe circumstiuee that Lm^' f " ^^ '"^'""y
organization the crown could not „« I "* constitution and
coSatitution or abrid^n, ?i. vLj' ",", * """' "' violating the
nolled and regutred^n^the co!, ^'^^ °1 "'° '"^^''^ '' ^as con-
owners and thdr atives /ts rkJ,Ve*7«1? fv,""** ^^ ""^ '=">'^
ing for their subsistence or „?J:!^!:::f:!.*l'!l^J:»^° »»' ■J«P'=nd.
crown; Its numbers and
sovereign. But the day h^'nassed when pr.C' ,• .-----
have any value. The fact of the Uii ^ v° "'^J^'^""" could
respects under the Cet cont 'l of I '^ T^ '^'"S placed iu all
to the crown but to pari aZ t i,lo If i- '^.^P^ns.ble not only
tional apprehensions'^undertM. head "«'' '° "^"'i""* ^"^ 'O""'--
CaSdrat^?:^it^i':reA°- ''^°f™/°''^» ''''''* -^
■e nr »,i^.„ ="'"=- uy men not aepend. officer a«;«t.H i:,, ■ . """" "^ command of a
-e or advancement upon the favour of the armv kn 1 if " »^ i ? "''j»'ant-general, belongin" to the
maintenance were beyond the royal control- ! ^.? appointed hy the queen. Tlie training of tl,7
statute. While the s^upreme coTmanS ;i irr"of°'tS""' "'■"• "'."' ''^"'? a mmury "^lege at K
e croivn. everv nn.<-H^,i .. :. ., !>everai ot the eovcrnino- b^r^,- o„.T _...i- !' , PT f"- '^
its goveriiment wily stTt^te WhUe'thrr"'' "" '°^'' ""*^°'! « matter of Scare^ ihJT-"- Tl>e train hi. of the offi ?,;!;
distinctly vested in the c^™ everi n«ct IT."' T""''"'* T"^ ^'^--a' of 1^0^^ boL Inf * 7''*^'^ "V ^' "^ingsto
~ch parish having throDtil of ' "^^ °^ "S?'^'" ""-i ^^'J-five
cost, Ind each ma^n balffi J- ""PP'^'ng volunteers at it^ own
P«y £10 to provTdTa 'itai^;"evr/"''"!? ■" "^» of serving to
pay was to £the sa^e a^ hat of the re'° l'""^ "^i' ^f service °the
or assembled for anXl trai^in! th! ^1 ^' '?'* "''"« enibodied
nnderthe Mutiny Act^idTuclfs o/wfrTi.?.°i"'" '^^^^
"PPreheXdTvS?" '!f,??.".ir:'» »". "«' ^e militia in
ca» of a;;;h n^dTvSror of ?^;:n'° "".""' ^» ■"■"«" '« r^' ^'' . !f '^ ^PP^^-l °^«^ t^; aVea on which the due^
Sf the militia b^Th" c o^he ^tiS^T'?' "^ nncpnstitutional use
each ye;>r, not by an e«?ut,ve !^ n"f ^°l '^ "^'"'"S ''as framed
the Ifouscof Commons Use f I W .If °f .' '« .^"ereign, but by
of the House, anTt was 'fl.i !!P^''-i-''' '"'"ative of a committee
of the militia for thrveTr te^t'"'/'''"-'''" l**''"'' ''"''•'"g
militia of England rem^ed fo?n ^'^ ^"""".K ^"^^tantially tht
militias being „°ean7ime brought nn'i^''.^ ^^' ^"^^ '"^ Scotch
various enictmeJ, TK. Z!"?''' ""'^!'- ^«. ««>« conditions bv
army. " ''ghtiug strength of the imperial
MILK is the fluid secreted by the mammal' gia^S rf
0^tL7 ""** "^dunentary form in the Monotremes Jta!
OmithorhyruJi-u» there is no nipple, but the mmiih J^
op^HnTtheT'^^P^nr^ '^' ^^- - Scrt^fdu^
oi^n, and the fluid is withdrawn by suction on the part of
LSf^ •*' il"'1 "^ *'•* g'*"'^ °P^" i^to a small poul'
foreshadowing !he larger pouches of marsupials. 1^
^nTJ^^^l' f'^ "« tno^compact, andTave atea£
number of lobules. They are found behind the mX'
t>-o on each side nor more than thirteen, six on each side
and one midway. The ducts, long and sle'nder d^i^^a^S
tion, open on a ninn e which ;» ^„„„,«j u_ . "^'°«/acta
. . . n « brought undeV7h''B«m'.'T"i";'''™'J" I ti«^ "•'■ • \"'= ""''"> 'ongaid slender during lacta-
various enactments. The force u-a.^miLi conditions by tion, open on a nipple which is covprpH \.^ = Z^^a-
during the last and in the eariv v^^^^"*' °° '"'""' """'"n^ 'he skin at the back of the nn^.b If P ■ "^^^^^O" "^
it contributed laigely to thea™Ve„I!„ 1 • '.r'ff" ""'"'•y. and hood or sWb T^ • . P? ''' *^"^ forming a kind of
1803 to 1813 Just 100.000 meTortf^^i.'" 'Vf """'"'»■ P^"" dim-n. 1 . »■ ^^°VP'e ^ protruded beyond the hood
'S^^h.^^r^SF^^^^-^^ tt:^niXTe^^\^rtirn't:tfn"utbe''? ""-^'^
-od:c--a«d"iHSf f -"- '-"ft^^^ sratrbi^^hX^-^^:
va uable functions. In the war^t^T,, •'"f ' " '°J"'" ""'t *' * ''"■'^> ^^ t^^^e" nipples Rodent, tbow „
agiiin called out ^It hS^l. fi'^'^J'"" "^^f"' ''•""="''"» 'vh" the oririnal «f^ ♦^u 7 '''*'"' *'"" ^^"^ ^""^ af>ont;
«>nu.l training: and wh"n"tLbri'l,/°-^t^i"'^ '^™'''^'' ^" onl v 3« . \ '^,\<J°'"«ti'= «Pecies breeds, however,
Aldershot and other 'camps of fnst^clon Tt'* '?•! ''^'" f°"=" "' d^^ ? annuaUy, and has but one to two youn? so the
proficiency have "enerallv .1! ;, i ?u ° ''^ military aptitude and domestic variety is a curious annmalTr ,1n^ f/fl J^ • ?
fessional solUie^" Jn^gn in?"* "".' ''"■'"■^'"' admiration of pro- circumstances of its i;f«^ T T ^ • ^ ^"^ artificial
n>ade. It waHart of the ^. '""■''"" '""'"'""o"*' change was nipnl^^B^rL ft- l''^ POrcupmes there are two
year that the control of the miUtilT "Iff"^ inaugurated if th^ S^,M^ "^tZ^ ^^^""^ ^^^ ^ore and hind leg, and lie
licuunant of the county anTveteJwholl vi'^'^r'^'^ '■^°"'*'' '»"» InLT^^ ^''''''° '^ ""^ "^« ^^^^ °f ^he^ fore leg
1^" virtually ceased to e'xist M a diTtWhodl '?* "^ " '"^ K 1 ,. "^^P!^ *" "^''^ oft®" •^■'lying its youna on ^
«.a re^r force, with'. Lmitati^on'tr ^^'^tiiL^lnd L^^and S^filt''' " TT ^T ri--. ^ teats ^prc^o^ctC
area and I the flanks near the shoulders, and are of considemble length
302
MILK
so that the young readily reach them. The Iiiseclivorn
have, as a rule, more nipples than are found in any other
order. Thus in the tenrec {CenteUs) there are as many as
twenty-two, and they are rarely fewer than fourteen,
spread out in pairs from the pectoral to the inguinal
regions. There are ten teats in the common hedgehog, six
to eight in moles and shrews, two in sloths and armadillos.
In Celacea there are two long, narrow, flat glands lying
between the dermal and abdominal muscles, with the sub-
cutaneous Uubber separating thera from the skin. The
peculiarity of the arrangement in these animals, where
suckling is performed under water, is the large size of the
central duct, which acts as a kind of reservoir, so that the
young may obtain a considerable supply in a very short
time. It would appear also that when suckling takes place
the nose of the young is above the surface of the water.
Among Ungulates, in the elephant the glands and teats are
between the fore legs; in the rhinoceros they are inguinal;
in the mare and ass the glands are two in number, and are
found between the thighs, about 9 inches in front of the
vulva; the tapir has two inguinal nipples, the peccary
two ventral and two inguinal, the wild sow eight nipples,
whilst in the domestic breeds there are at least ten, extend-
ing from the pectoral to the inguinal regions. Ruminants
have the glands aggregated into a round mass in the
inguinal region, pendulous in full function, divisible into
two glands, each of which has a large reservoir. ^Mien in
use the teats, one pair or two pairs being the number, in
connexion with the reservoirs become so large as to receive
the special name of " udder." All the deer tribe, camels,
the giraffe, and all kinds of cows have four teats ; most
antelopes and the gazelles have two teats, whilst a few
antelopes have four. As to Cariiivora, the felines have
usually six nipples ; the wolf, jackal, fo.x, dog have usually
eight ; the seals and the walrus have four, the otters
two, the weasels six, the bears six ; and in the kinkajou
(Cercoleptes) the number is reduced to two. Amongst
Quadnimana, the aye-aye (Ckiromt/s) has only one pair of
nipples, about an inch and a half in front of the vulva ;
many lemurs have in addition to those a pectoral pair ; in
all the platj-rhine and catarhine Quadntmana there is only
one pair of glands, restricted to the pectoral region. Here
the teats are between the fore legs, and the young clings to
the mother's breast in human fashion, but there is no protru-
sion of the breast as in the human being. -(For further
details see Owen's Anatomy of Vertebrates, vol. iii. p. 7G9.)
In the human race the glands are two in number, form-
ing, along with the skin and fat, two rounded eminences,
one on each side, on the front of the thorax. They extend
from the third to the sixth or seventh rib, and from the
Bide of the sternum to the axilla. In the centre projects
a small conical body, the nipple. Around the nipple is a
coloured circle, or areola, which is darker during pregnancy,
and even in women who have borne children than in the
virgin state. The surface of the nijipls is ^^Tinkled, 4nd
with a magnifying glass is seen to be covered with
papilla;. It is perforated by numerous openings, the mouths
of the milk ducts. The tissue of the hippie contains
numerous minute blood vessels, and it has at the base
muscular fibres arranged in concentric circles and in
radiating bands. I', has much of the character of erectile
tissue, as in the corpora cavernosa of the penis, becoming
turgid, firm, and prominent from excitement. The base
of the gland lies on the pectoral muscle, a thin layer of
fascia intervening. The surface is covered with fat, which
gives it the smooth rounded outline. It is amply supplied
with blood by the long tlioracic artery, some other minute
branches of the axiPary artery, the internal intercostal
artery, and the subjacent intercostal. The nerves come
from the anterior and middle intercostal cutaneous branches,
and the nipple is e.specially sensitive. The gland is com-
posed of numerous lobes bound together by connective and
adipose tissue, and each lobe is formed of smaller lobules.
Each lobe has an excretory duct, and these ducts, from
fifteen to twenty in number, converge towards the areola,
beneath which they are dilated so as to form sinuses from
Jth to ith of an inch in calibre. From these sinuses arise
the ducts which 0|)en on the surface of the nijiple. Tho
general structure Avill be imderstood by referring to tho
accompanying figures, along with the description.
Flo. I. — HalMlnprammntic view ef a section (Iirough a lobule of the ntflm*
m.iry gliind, after Klein {Al'Cis of nhlolo^y. pl;i!e xl. fig. 1). macnlfled W
diameters, a. n duct dlvtiUne Into two binnehes; t.b.b. conneriive tissue
surrounding and going between tlie uUimalc pontiles of tlie plnnd: e. c. f, tbe
pouches or altcoli uf tlic gland, the dots representing tlie cells liping tbcm.
Fro. 2.— A portion of the snine gland, magnified about 400 diameters, showing one
complete and two Incomplete alveoli, a, rt.o, short, columnar, eplllieliul cells
lining tile alvcolu^ each liaving an oral or rounded nucleus; ft, 6. 6, epithelium
cells, containing, next liie interior of the alveolus, a mllli globule; c,e,r,e, roUk
globules wlJcli h.ivc been set free from epllhelini cells.
When a duct is traced into the gland, it is found to sub-
divide into smaller ducts, and these into still smaller, until
the smallest ductlet is reached, round the end of which are
clustered several alveoli or pouches. Each alveolus lias
a wall, lined with epithelium cells. In the wall of the
alveolus there are capillary blood-vessels which bring the
blood near the cells. By this blood the cells are nourished.
There is a minute cavity in the centre of each alveolus into
which cells or their products can accumulate. There can
be no doubt that the formation of the milk globule takes
])lace in these cells. Whilst milk is not being formed the
cells have a gi-anular appearance, and the lumea or central
cavity of the alveolus is small ; but during secretion tho
cavity is enlarged and shows a few milk globules, whilst
one or more milk globules can be seen in the interior of
tho cell. If the milk globule in the cell be very large, the
nucleus of the cell is pressed outwards and the proto|>lasm
of the cell is reduced to a thin covering, over the globule,
at this stage presenting a striking resemblance to a fat
cell containing an oil globule. Tlius each milk globule is
formed in the protoplasm of the epithelium cell, and even
at an early stage each milk globule consists of a minute
drop of fat or oil surrounded by a thin albuminous envelope.
It has not been clearly ascertained whether c]iithelial cells,
after having- sci-retcd milk globules, degenerate and fall
' off, or whether they have the powtr of ejecting the milk
' globules. Tho fluid constituents of milk (water holding
MILK
303
iialta in solution) may be separated rroni the blood by a
kind of filtration under blood pressure, as is the case in
other secretory processes. The origin of the sugar of milk
and of .the casein is unknown. (For a description of the
minute structure of the
milk gland, see Klein's
Atlat of Histology, p.
300, and raferences.)
At the beginning of
lactation the milk is
rich in large irregularly-
formed corp'.iscles (fig. 3,
a, a, a) called colostrum
corpuscles. These are
contractile bodies, slow-
ly changing their form
and squeezing out the
oily particles. At first Fio. 3.— a drop ot mUlt magnieed 300 dluiieten.
they are the only bodies "■ '•'^ """"""' "'T""^''-
present, but they are soon replaced by the ordinary milk
globules. Such globules have bright refractive edges,
2ie surface is smooth, they vary in siie from g ^'o o^^ *°
'g^^th of an inch in diameter, and each consists of a
drop of fatty matter surrounded by a laver of albumen
("Ascherson's membrane ").
A secretion of mUk takes place in ijewly-bom children,
from the fourth to the eighth day, and also in rare cases
in men (Hermarm's .f Ay^'o/oyy, p. 158). During gestation
in the human being the mammary glands increase in size ;
immediately after the birth of the child active secretion
commences; and usually it is on the stoppage of the secre-
tion, ten months afterwards, that the process of menstrua-
tion, which has been arrested by impregnation, again is
re-established.
The secretion of milk is undoubtedly affected by the
nervous system, as is shown by fear or mental distress
arresting or injuring the quality of the secretion, and by the
" rush " or feeling of fulness in the breast e.xperienced by
the mother when the child's mouth touches the nipple, or
even when she sees her offspring. The nervous mechanism,
however, is unknown, as it has been observed that secretion
may continue even after section of all the nerves known to
pass to the gland. The nature of the diet has a marked
influence on the quality of the secretion. Thus the
amount of casein and of fat is greater during an animal
than during a vegetable diet. Fatty foods do not seem to
increase the amount of fat or butter ; an ample supply of
earbo-hydrates (starches and sugars) increases the amoimt
of sugar. These facts indicate that most if not all of the
constituents of milk are formed from changes in the pro-
toplasm of the epithelial cells. In some women the nulk
is deficient in fat and casein, and consequently is less
nutritious. Prolonged lactation diminishes the amount of
fat and sugar without materially affecting the amount of
albuminous matter ; but the milk is less nutritious and is
unfit for the child. The occurrence of menstruation during
lactation also deteriorates the milk. ^j. g. u.)
Milk as Food.
The milk of various domesticated animals is more or less
used by man for food. The milk of the cow, which may
be taken as typical of all others, and is indeed by far the
most important and valuable of all, is, when newly drawn,
an opaque white fluid, with a yellowish tinge, soft, bland,
and sweetish to the taste, and possessed of a faintly animal
odour. This odour, according to Schreiner, is due to the
presence of sulphuretted hydrogen, and disappears after a
short exposure. The specific gravity of milk ordinarily
ranges from 1-.029 to 1 033, very -seldom reaching 1035 or
falling so low as 102 7. In chemical constitution it con-
sists of an emulsi'on of fatvy globules (cream) in a watery
alkaline solution of casein, and a variety of sugar, peculiar
to milk, called lactose. The fat (which when separated we
know as butter) and the lactose constitute the carbonaceooa
portion of the milk regarded as food. The casein, which
forms the principal constituent of cheese, and a certain
proportion of albumen which is present, form the nitro-
genous, while the complex saline substances and water
are the mineral constituents. These various substances are
present in the proportions which render milk a perfect and
tj'pical food suitable to the wants of the young of the
various animals for whom it is provided by nature. The
milk of all animals, so far as is known, contains 'hem,
although they are present in somewhat different propor-
tions. It is probable that the nulk of ruminants possesses
certain physical and physiological distinctions from that of
non-ruminant animals, which will account for the virtues
attributed to the milk of the ass and mare. The following
table exhibits the chemical constitution of the kinds of
milk most frequently used by man : —
Cow.
Goat
Ewe.l
Mare.
Ass.
Hainan.
i
1
1
>
1
1=1
1
Water
Fat
86-87
3-50
ji75
4-00
070
87-00
4-00
4-10
4-28
0-62
84-48
6-11
3-94
4-68
0-79
83-70
4-45
518
5-73
0-96
90-310
1-055
1-953
6-285
0-369
91-65
0-11
1-82
6-03
0-34
88-02
2-90
1-60
7-03
0-31
Casein and
albumin...
Sugar
Ash
In addition to these constituents milk contains small pro-
portions of the gases carbonic acid, sulphuretted hydrogen,
nitrogen, and oxygen, and minute quantities of other prin-
ciples, the constant presence and essential conditions of
which have not been determined. These consist of galactin
and lactochrome, substances peculiar to milk, discovered
by Winter Blyth, with certain animal principles such as
leucin, pepton, kreatin, tyrosin, <S:o. The salts in milk
consist, according to the average of numerous analyses by
Fleischmann, of the following constituents: —
Phosphoric acid 2831 Potash 173*
Chlorine 1634 JIagnesia 407
Lime 2700 Ferric oitide 062
Soda 10-00
Milk thus is not to be regarded as a definite chemical
compound nor even as a mixture of bodies in fixed and
invariable proportions. Not only does the milk of different
races and breeds of cows vary within comparatively wide
limits ; the milk of the same animal is subject to extensive
fluctuation. The principal causes of variation in the
individual are age, period of lactation, nature and amount
of food, state of health, and treatment, such as frequency
of milking, ic. The following table indicates the range
of normal variations: —
■Water 90 00 to 8365
Fat 2-80 „ 4-50
Casein and albomiji 3-30,, 5-55
Sugar 300 „ 550
Ash 0-70 „ 0-80
The average quantity of milk yielded by cows is also
highly variable, both in individuab and breeds. As a
rule the smaller breeds of cows yield a small amount of
milk rich in cream (butter fat), while the yield of the
larger breed is greater in quantity, but comparatively
deficient in cream. A good milch cow should yield in
a milk-giving period of from eight to nine months about
' Ewo'a milk is exceedingly variable, especially in its percentage of
fat. The above analysis is one of nine by Dr Voelcker, in which
the fat was found to range from about 2 to 12^ per cent.
304
MILK
500 gallons of milk, from which nearly 600 ft of cheece
or 200 B) of butter would be obtainable.
Dairy Treatment. — Ciows are commonly milked by hand
two or three times a day. A milking machine of American
origin, which was introduced about the year 1862, has been
entirely abandoned. The milk should be drawn from the
animals in as clean a condition as possible, but notwith-
standing every precaution some amount of hair and
epithelial and other animal debris invariably enters the
milk-pail. It has therefore' to be immediately strained
through a sieve with fine wL'e-cloth or hair strainer. As
milk is peculiarly susceptible of taint, and absorbs odours
of all kinds with great avidity, it is of the utmost con-
sequence that all vessels in which it is placed or kept
should be so made as to be easily purified and that
they should be kept scrupulously clean. In Switzerland
milk is strained with most beneficial effect through sprigs
of washed fir tops, which inserted loosely and uprightly
into the hole of a funnel arrest all hair, skin, clots, and
8limy matter on the acicular leaves. The Tnilk drains
through in a clean condition with a fresh slightly
aromatized flavour favoui-able to its keeping. A fresh
^rig is used on each occasion of straining mHk, so that
there is freedom from the risk of taint which arises through
the use of imperfectly cleaned wire gauze. The milk milst
be removed froM the cow-house as quickly as possible ;
and, if intended for use as new milk and for sale in the
neighbourhood of the dairy, it may at once be put up for'
delivery. But if it has to travel a distance, or if it is to
be kept for creaming or cheese-making, it should be rapidly
cooled down, and kept in a cool airy milk-room if prac-
tica,ble, surrounded with fresh cold water.
The ordinary method of separating cream either for
direct use or for butter making is by allowing it to form
on the surface and skimming it off with a broad flat spoon ;
but ingenious adaptations of centrifugal machines — of
which Laval's separator b one of the best known — have
been introduced for the purpose of effecting the rapid and
complete separation of the cream. The centrifugal force
of Buch machines throws the denser portions of the fluid
towards the sides of a rapidly revolving cylinder, collecting
the cream on an inner layer, which is carried off by one
channel while the impoverished milk escapes by another.
The Laval separator gives very rich cream, as will be seen
from the following analyses by \oelcker : —
Ordinary
Cream.
Cream by
Separator.
Skimmed MUk
by Laval
Separator.
Ordinary
Skiiwned
MUk.
Water
77-80
15-45
8-40
3-15
0-70
66-12
27-69
2-69
3 03
0-47
90-82
0-31
8-31
4-77
0-79
89-25
1-12
8-69
D-16
0-78
Mineral matter
After being kept some time, depending principally on
the temperature at which it is maintained, niilk_ begins to
turn sour owing to the formation of lactic acid, by a
process of fermentation, at the expense of the lactose or
milk sugar. The acid so developed causes a coagulation
of the casein, and the milk separates into a solid white
curd, and a thin transparent yellow milk serum or whey.
These changes can to a certain extent be artificially pro-
duced, hindered, and controlled. The following are the
results of analyses by Fleischmann : —
ConatiUtenls of 100 Parts of Sweet Milk. ,
i 3-56 butrtf:
20-00 cream < 16 30 buttermilk.
/ 0-14 loss.
( 7 '93 card,
79-70 ekimmed milk < 7145 whey.
( 0-32 losa.
0-30 loBS 0-30 loia. '
lyiatlK Compcsition of itUh and Us Prodx.ctn.
Wat«r.
Fsl.
Caaeln.
Albomin.
HlDi
Sagar.
^
AA-
^Vllolemilk
87-60
77-30
90-34
14-89
91 00
59-30
94 00
8-98
15-45
1-00
82-02
0-80
6-43
0-35
3-02
3-20
2-87
1-97
3-50
24-22
0-40
0-40
0-20
0-45
0-28
0-20
3-53
0-40
4-30
8-16
4 63
0-28
3-60
5-01
4-65
0-70
0-70
0-71
0-56'
0-70
1-61
0'€0
Skim-milk
Curd ;
Wley
The simplest and most advantageous form in which
milk can be disposed of as a commercial product is by ita
sale as sweet or new milk, and it is in this manner that
the greater proportion of the milk produced within tho-
reach of largo centres of population is disposed of. New
milk, cream, and skimmed milk are the only primary forms
in which milk is sent into the market. Cheese and
Butter have been dealt with in separate articles (q.v.).
AVhey, the yellow liquid remaining after the separation of
the curd in cheese making, is a source of milk sugar,
employed to a limited extent in pharmacy ; but it is prin-
cipally used for feeding pigs. The bui.,crmilk which re-
mains after separating butter is a most wholesome and
nutritious article of food.
Preservation of Milk-— The niunerons methods which have bean
proposed for tho presei-vation of milk in a condition fit for use over
a lengthened period resolve themselves into (1) diemical treatment
with alkaline salts and antiseptic bodies, (2) physical tieatjnent,
Euch as cooling or icine;, boiling, and aeration, ana (3) condensation
with or ■without tho addition of a prescrvativo agent. AH system*
of preservation, however, are subject to serioiis disadvantages either
from their serving their purposa for too limited a time, or their
interfering with the natural constitution and properties of tho
milk. Of aU preservatives cold is the most efficient and least
objectionable. It has been shown by Soxhlet {Dingler's PolytccK
Journal, ccxxiii, 329) that nulk cooled by ice-water remains sweet
and unaltered for fourteen days, but after that time j.cquirefl a
rancid taste. After twenty-eight days it coagulates on boiling
owing to the presence of acids resulting from the oxidation of the
cream, and in thirty-four days it coagulates even in the ice-wator.
It is also found that milk which has undergone aeration witt
atmospheric air has its keeping properties much improved. The
aeration is effected by allowing the milk to fall from some height
in a state of fine division by passing it through the meshes of a
sieve. By another method air cooled by passuig over ice is blown
through the milk.
Jtilk keeps sweet for a longer time when boiled, bnt the smell,'
raste, and other properties are atfected, partly owing to the escape
of gases mixed with it when fresh. The unpleasant flavour com^
municated by boiling can be avoided if the action takes place in a
closed vessel and the milk is immediately cooled down in a
refrigerator connected therewith. In the case of any suspicion of
taint in milk either from ilisease in the cow, contamination from
unhealthy persons, or the use of infected water in cleaning vessels*'
boiling is also btroiigly to be recommended, as it effectually
destroys the genus of disease^ in the carrying and -spreading oif
which milk is a most active agent. It is witli uie utmost difficulty
that boiled milk can be coamilatcd by means of rennet ; but b^
treatment with acid it coagulates more rapidly and freely than if
unboiled.
Of tho various chemical compounds which have been suggested
and more or less used for preserving milk, the most successful
liitherto has been salicylic acid, which has the advantage of being
tasteless and inodorous. By biiskly stirring in rather less than »
grains to a pint of milk, it can be kept liquid and sweet in a tem-
perature of from 65° to 68" Fahr. for twelve hours, and at 55'' Fahr.
for a whole day. If 4 grains bo used to a pint, coagulation in the
higher temperature is delayed from two or three days, and at th©
lower temperature the milk may be kept good from three to five days.
Boracic acid and borax are also employed by dair)'men, the former
being known as glacialino salt. The presence of any chemical anti-
septic in milk is, however, at best a matter of doubtful advantogcw
ComUnsatioTi. — Milk is now treated on a large scale by a process
of concentration, tho product of which cornea into the market in
two forms — as " plain condensed milk " and as " pro.«»crved milk."
Tho credit of originating tlic industry is due to Mr (Jail Borden of
Uhitc Plains, New York, who began his experiments about ]849.
Ill 1851 ho introduced his plain condensed milk, which is simply
milk fr«m wliich between three-fourths and four-tlftbs of the wat,er
lia« been removed, and in 1861 ho rendered important .services to
the army in the fitld b^ supplying preserved' milk which was lot
MILK
805
effect milk aimilarly concentrated, with a proportion of sugar
added, and hermetically sealed in tin cans. The manufacture was
transplanted to Switzerland in 1865, after which condensing
factories were estahlished in England, Ireland, Denmark, Bavaria,
Norway, and elsewhere. With the introduction of the condensing
OTidc there has also heen associated the factory system of dealing
with daily products, by which the milk of many dairies is carried
(0 one centre and dealt with either for condensing or for cheese or
butter making. The following epitome of the process of condens-
ing milk is from a paper by Mr Willard of Cornell university,
New York (Jour. Jioij. A(jric. Soc, 2d series, vol. viii., 1872).
Tiic milk when received at the factory is iirst passed, he says,
" through a strainer to the receiving vat ;. from this it is conducted
off, going through another strainer into the heating cans, each
holding about 20 gallons ; these cans are set in hot w.iter, and the
milk is held in them till it reaches a temperature of 150^ to 175°
Fahr. ; it then goes through another strainer into a large vat, at
^he bottom of which is a coil of copper pipe, through which steam
is conducted, and here the milk is heated up to the boiling point.
Then the best quality of white granulated sugar is added, iu the
proportion of 1} lb of sugar to the gallon of milk, when it is drawn
into the vacuum-pan having a capacity of condensing 3000 quarts
or more at a time. The milk remains in the vacuum-pan subjected
to steam for about three hours, during which time about 75 per cent,
of its hulk in water is removed, when it is drawn off into cans,
holding 40 quarts each. The cans are only partially filled, and are
then set in a large vat containing cold water, the water being of a
height equal to that of the milk in the cans. Hero it is stirred
until the temperature of the condensed fluid is reduced to a little
below 70°; it is then turned into large drawing-cans with faucets,
in order to facilitate the tilling of the small cans holdin"
1 lb each, which are immediately soldered to exclude the air."
In the ease of plain condensed milk the concentration is usually
carried farther than is practised in preparing the preserved milk, it
being evaporated down to between one-fourth and one-fifth of the
origin.al bulk. Ii is not put up in sealed tins, being intended for
immediate use, and keeps sweet only for a few days, varying with
the state of the weather, whereas the sugared milk in sealed cans
keeps for years. The large amount, however, of cane sugar added
to preserved milk seriously disturbs its balance of proportion as a
perfect food, and renders it unfit to be used alone in a dilute state
as a substitute for mother's milk by infants, a purpose for wliich it
is largely employed. It should also be observed that the relative
proportion of fat is small, the milk being partially skimmed before
it is operated on, so that the statement that preserved milk diluted
with a small proportion of water is equal to cream is not to be
relied on. Preserved milk, rich in cream, has always a more or
loss rancid oily taste, and cannot be obtained so sweet and even in
flavour as that largely deprived of fat. According to a German
patent of E. Klebs in Prague, plain condensed milk may bo
preserved by adding to every 100 litres of the original milk a
solution of 50 grains of benzoate of magncsiuir iu oua litre of
water.
Adidlcralion. — Practically the invariable mode of sophisticating
milk for sale cosisists in the addition of water and iu the subtrac-
tion of cream,— iu other words, passing olf skimmed or partlv
skimmed as new milk. Now and again there are found certain
little refinements on these simple frauds, such as adding a quantity
of sugar to correct the specific giavity. Hour or starch to increase
opacity, and a touch of colouring matter to cover the bluish tinge
wliich would betray skimmed milk. In the United Kingdom no
ofticial standard of what constitutes pure milk has been promul-
gated, but the so-called Somerset House standard has been
generally recognized in law courts. According to this, new milk
should contain as a minimum of solids not fat 8 '6 per cent, and of
fat 2-5 per cent., and of water a maximum of .83-9 per cent. The
most satisfactory manner of discovering the probable genuinenr-
of a sample of milk is by chemical analysis carried suHiciently 1. .
to determine the amount of fat and of other solids present,
lyumerous attempts have been made to place in the hands of dairy-
men, dealers, and consumers of milk a trustworthy method of
■estimating the condition and value of the article by simple
nuautitive tests for cream or fat — at once the most valuable con-
stituent and one the presence of wliich in average proportion is
indicative of the quality of the whole. The simplest but at the
same time the least trustworthy and efEcient method is by means
of the so-called "creamometer,'' which consists merely of a
graduated glass tube in which a measured amount of milk is placed
and the amount of cream it throws up is read off by means of the
scale. Specific gravity determinations have by themselves no
Significance, seeing milk deprived of its cream can by dilution with,
gatei- be brought to correspond exactly with the original milk.
But by a combination of two methods,— first taking the specific
gravity, next observing the yield of cream by the " creamometer,"
and finally taking the specific gravity of the milk deprived of
cream, regard being had to the temperature of the milk in these
observations,^ an approximately accui'ate idea of^the .value of_a
1(>— 13
sample may be obtained. Among so-called "lactoscopcs," the
operations of which are based on the fact that milk rich iu cream
IS a much more opaque fluid than that from which cream has been
taken or to which water is added, that invented by Professor
Fescr of Jhinich is one of the simplest and most useful. It aon-
sists of a glass tube open at the u\<],er end and attenuated it ■US
lower extremity. Into this narrower portion is fused a sttail
cylindrical rod of opaque milk glass on which black Hues ai-e
marked. These lines are invisible when the lower portion of the
tulie is lillcd with a measured quantity of niilU, but on ailditioii ul
water they become visible. \\"lieii the black lines become bv the
gradual admbituie of water perfectly distinct, the richurss of the
milk in cream globules is indicated by the height to which the
mixture of milk and water has risen iu the wide portion of the
tube, which has engraved on it a scale showing on one side the
amount of water added and on the other the jivoportion of cream
equivalent to the transparency resulting from such addition.
Stalistics.— In the year 187S it was calculated by llr J. C. Jloiton
that the total yield of milk from the 2,250.000 cows and heifers
in milk or in calf in England and Scotland amounted to about
1,000,000,000 gallons yearly. He assumed that about one-sixth o£
that quantity (107,000,000 gallons) went to feed calves, and that
the daily consum)>tion of the population was 1,000,000 gallons,
being rather more than a quarter of a pint per head, which aceouiiis'
for 305,000,000, still leaving 468,000,000 t.iUons to be used for
butter and cheese making. Two-thirds of this quantity, or
312,000,000 gallons, Jlr Morton assumes was used lor cheese-making,
yielding 2,800,000 cwts. of cheese (rather less than 1 lb per gallon
of milk), and the remainder, 156, 000,000 gallons, of milkdcvotid to
butter-making would yield 530,000 lb of butter, or 1 lb of butter
for every 21 pints of milk. In these figures no accouut is taken of
Ireland, whence at that period there were sent to England alone
yearly 3,500,000 lb of salted butter. In June 1882 the number of
cows and heifers in milk and in calf in Great Britain did not vary
greatly from the number on which Mr Morton's estimate for 1873
was based, being 2,267,175, whilst in Ireland the number w.ns
1,398,905, making the total for the United Kingdom 3,682,317.
If we take approximately ilr Morton's data as the basis of calcu-
lation, the 3,682,317 milk cows and heifers in the Uuited King-
dom would yield, at 440 gallons per head, 1,620,219,480 gallons
of milk. Further, assuming that one-sL\tli of this is consumed
by calves, one-third consumed by population, one-third used for
cheese-making, and oue-sixtli used for butter-making, we have as
the yield of cheese 4,846,000 cwts. and as the yield of biittrr
920,000 cwts. As Ireland is much more a butter-producing th.in a
cheese-yielding country, the quantity of cheese made is prob.ibly
overestimated in these figures, and the amount of buttrr niade is
correspondiugly understated. To bring out the consumption ol^
dairy products for the year the following imports must be added: —
Cwts.
1 Vilec.
2,1C;,4:'3
11,S3U,-.'JC
Thus we finil tlie total suiii-]y of cheese to tlie Uuited Kini^dont
iu 1SS2 was 6,538,495 cwts., au.l of butter the supply was Z,Ob7,4:S
cwts. Estimating the liouie produce of both articles at the same
value as the imports, the cheese supply cost £18,320,000, and
the butter £16,150,000. Adding to these the probable cost of tha
milk consumed as such (say 550,000,000 gallons at Is. per gallon
= £27,500,000), we have for the year 1882 iu round uunibeis
£62,000,000 expended on dairy produce within the United Kingdom.
The total number of milch cows at present (18S3) iu the United
States is stated at 15,000,000, which, taking the 440 gallons basis,
yield annually 6,600,000,000 gallons, or nearly 30,000,000 tons of
milk. In America the factory system of treating milk has attaincil
much greater dimensions than in Europe, and that perfection of
: ;catnient, combined with the cheapucss of raising and feeding stock,
enables the American companies to enter the European markets
with large quantiticsof cheese and other dairy products of uniformly
good quality which find a ready and remunerative sale.
K oil miss.— V nder this name is properly understood a feraiented
drink prepared from mare's milk by the Tartar tribes of the Russian
empire and by all the nomad races of the northern parts of Asia.
It is made by diluting mare's milk with about one-sixth piart of
its quantity of water, and adding as a ferment about one-eighth
part of very sour milk or of old koumiss. This mixture is placed
in a wooden vessel which is covered over with a thick cloth, and-so
left for about twenty-four hours in a moderately warm situation.
Dui-ing that time a thick coagulum rises to the surface, which is
thoroughly i-eincorporated by churning. After standing for another
day, the whole mass is again thoroughly chmned and mixed up,
and in this state it forms new koumiss, having an agiceable subacid
taste. The liquor is mostly stored and preserved by the Tartai-s in
skin bottles, in which the fermentation continues developing ii >
alcolwlic qualities, and mellowing and improving its taste. Genuir i
Tartar koumiss has the follu>\ing composition :— alcohol^3'21, lactl:;
806
M I L — M 1 L
.-.cid 0'19, sngar 2-10, albuminoids 1'86, fat 178, salts 0-509,
carbonic acid 0-177, and water 93-40. A distilled spirit is i)repared
from koumiss, which is drunk among the Tartars under the name
Ktl araca or arsa. Koumiss has of late years come into prominent
notice as a remedial agent in cases of pulmonary consumption, and
generally as a nutritious form of food easily assimilated by delicate
stomachs. It is prob.-ible that all its virtues reside in the original
milk from which it is prepared, in w-hich case the koumiss can only
be regarded as valuable in so far that it is a convenient form under
which the essential properties of the milk can be preserved for use.
Under the name of Kouraiss a preparation of cow's milk is now very
generally sold. It is made by adding lo each quart of new milk
about a tablespoonful of common sugar and brewer's yeast, allowing
the fermentation to proceed a sufficient length, then bottling and
corking as in the case of aerated waters. Such a preparation con-
tains about the same proportion. of alcohol as genuine koumiss, but
a non-alcoholic variety can also be obtained, made by a process of
natural fermenfation, which continuing after bottling develops
a krge amount of carbonic acid and renders the liquor highly
efl'ervescent. (J. PA.)
MILL, jAJfES (1773-1836), historian and political and
mental philosopher, was born 6th April 1773, in the
little -Tillage called Northwater Bridge (Bridge of North
Esk), in the parish of Logie-Pert, in the county of Forfar.
His father, J -imes Mill, -was a shoemaker ; his mother,
Isabel Fenton, belonged to a race of respectable farmers.
The father was industrious, good-natured, and pious, hut
not kno■^vn as specially intelligent. The mother was of a
proud disposition, and resolved to educate James, her eldest
son, for a superior destiny. He began his education at
the parish school, and went on to the Montrose Academy,
"where he remained till the unusual age of seventeen and a
ia!f, when he went to the college of Edinburgh (1790).
jiccording to the usage of the time and neighbourhood, he
ought to have been sent about thirteen or fourteen to
Marischal College, Aberdeen. His remaining so long at
the Montrose Academy, and his going to Edinburgh for
his university course, must be connected -with his being
taken up by Sir John and Lady Jane Stuart of Fettercairn,
who engaged him to be tutor to their only daughter,
!ino-mi for having inspired the affection of Sir Walter
Scott, and for being the mother of Principal James David
Forbes. Sir John and Lady Jane Stuart contracted a
warm attachment for Mill, which lasted throughout their
lives. At Edinburgh University Mill was distinguished as
a Greek scholar. But he received his greatest impulse
from Dugald Stewart, for whom he always expressed
-unbounded admiration. In October 1798 he was licensed
as a preacher, but seems to have preached very seldom.
His years from 1790 to 1802, besides being occupied with
incessant studies e.xtending into history and moral and
political philosophy, were devoted to various tutorships.
Failing to find a career to his mind in Scotland, in 1802
lie went to London in comnany with Sir John Stuart,
then member of parliament for Kincardineshire. He soon
obtained literary occupation, to which he applied himself
with untiring energy. His first important venture was to
start a periodical on a new plan, entitled The Literary
Journal, which began to appear in January 1803, and
continued under his editorship till the end of 1806. It
was the most comprehensive in its aims of any periodical
hitherto in existence, being a summary view of all the
leading departments of human knowledge. Thomas
Thomson, the chemist, took charge of science ; and many
other men of ability co-operated. Mill himself wrote
largely in biography, history, political philosophy, political
sconomy, and also in theology, on which his views at the
;irae were broad -wifbout being sceptical. The publisher
of the journal was Baldwin, who -\vas also the proprietor
■of the St Jamcis Chronicle, a Conservative paper appear-
ing three times a week. For two or three years, from
1805 onwards, Mill was editor, but at last gavo it up,
1 artly on conscientious grounds, although in conducting
it he never lent himself to the expression of any illiberal
views, but often made it the vehicle of the opposite.
In 1804 he -wrote a pamphlet on the Corn Trade,
advocating the impolicy of a bounty on the exportation of
grain. This was the beginning of his career as 'a political
economist. In 1 805 he pubiished a translation of Villers's
work on the Reformation, an unsparing exposure of the
vices of the papal system. He added notes and quotations
by -ft'ay of confirmation of the author's -views. On this
subject also he contmued to hold strong opinions all through
life, and often recurred to it in his articles in the reviews.
In 1805 he married Harriet Burrow, whose mother, a
-widow, kept an estabUshment for lunatics in Hoxton. He
then took a house in Rodney Street, Peutonville, where his
eldest son, John Stuart, was born in 1806. It was about
the end of 1806 that he entered upon, the composition of
the History of India, which ho expected to finish in three
or four years. He was actually engaged upon it for twelve,
giving, however, a considerable portion of his time to other
writing for the support of his family. The strain upon his
energies for those years was enormous.
He became acquainted with Jeremy Bentham in 1808,
and was for many years Bentham's chief companion and
ally. In 1810 Bentham, to ha\e Mill nearer him, gave
him Milton's house, which adjoined his own, and -n-as his
property. After a few months' trial ilill had to give up
this house on account of his wife's health, and went to live
in Newington Green; but in 181-1 Bentham leased the
house No. 1 Queen's Square, now 40 Queen Anne's Gate,
■lose to his own garden, and gave it to Mill at a reduced
rent; here he remained till 1831. The intimacy with
Bentham was rendered still closer. For four years, from
1814 to 1817, Bentham was at Ford Abbey, near Chard,
in Somersetshire, and there Mill and his family were
domesticated -with him nine or ten months each ;, ir, — in
which retirement it is probable that Mill was able to
accelerate the completion of his history.
In the twelve years between 1806 and 1818 he -wrote a
great many articles for various periodicals. Among these
were the Anii-Jacohin Revieiv, the British Eencio, and the
Eclectic Seviev) ; but there is no means of tracing his con-
tributions. In 1808 he began to -write for the Edinburgh
Revietv, and contributed steadily tilll813,mostofhis articles
being known. In the A nnual Eeiiew for 1808 two articles
of his are traced — a " Review of Fox's Historj'," and an
article on "Bentham's Law Rcfonns," probably his first
published notice of Bentham. The first known article in
the Edinhirgh was on " Money and Exchange " (October
1808). In 1809 (January and July) he wrote at great
length on Spanish America and General Jlirauda, -with
whom he was on terms of intimate friendship. In the July
number he also wrote on China. In 1810 (April) he made
a severe attack on the East India Company. He also
-wrote on the hberty of the press and on the Church of
England in connexion with the Lancasterian schools. Ho
was an active member of the committae for promoting
educatinn on Lancaster's plan. In 181 1 a periodical named
the I'hilanthrnpist was started by AVilliam Allen, and
published in quarterly numbers till 1817. Mill co-operated
with Allen boih in the writing and in the management.
He contributed largely to every number, — his principal
topics being education, freedom of the press, and prison
discipline (under wliich ho expounded Bentham's "Pajiop-
ticon "). He made powerful onslaughts on the church in
conne.xion with the Bell and Lancaster controversy. In
1814 Macvey Napier engaged him to contribute to the
supplement to the fifth edition of the Encyclopstdia
Britannica. Many of the atticles became notable. The
list included "Government," "Jurisprudence," "Liberty
of the Press," "Prisons and Prisoa Disciplind^" "Colony,"
MILL
307
•"Law of Nations," "Education," "Beggar," "Benefit
Societies," "Banks for Savings." In "Jurisprudence" and
"Prisons" he was largely indebted to Bentham; in most
of the others he was either altogether or in great part
original. The article on "Government" will occupy a
permanent position in' English history.
In 1S18 was published the History of India, which had
a great and speedy success. It was the means of changing
the author's future position. The year following he was
appointed an ofScial in the India House, in the important
department of the examiner of Indian correspondence.
He gradually rose in rank tiU he was appointed, in 1S30,
head of the office. He introduced his eldest son into the
same department in 1823.
In 182'1 Bentham projected the WestrntTister Review, and
Mill was a principal writer for three years. Some of his
most vigorous writings are included among those contribu-
tions. The first was an elaborate criticism of the Edinburgh
Revieio as a whole ; it was followed by an onslaught on the
Quarterly. Other articles dealt with English history and
with ecclesiastical establishments, which he severely im-
pugned. To a periodical of short duration. The Par-
liamentary History and Review, he contributed an elaborate
political retrospect of the parliament of 1820-26. In
1829 appeared the Analysis of the Human Mind. From
1831 to 1833 he was largely occupied in the defence of the
East India Company during the controversy attending the
renewal of its charter, he being in virtue of his office the
spokesman of the court of directors. In 1831 Sir WiUiam
Molesworth projected the London Review, and Jlill con-
tributed to it during the last two years of his life. His
most notable article was one entitled " The Church and its
Reform," which was much too sceptical for the time, and
injured the Review. His last published book was the
Fragment on Maekinlosh, which appeared in 1835. He
died on the 23d June 1836.
A considerable space would be required to do justice to Mill's
character — intellectual and moral — as shown both in his writings
and in his intensely active and influential carter. He was an ex-
cellent scholar, in the sense of knowing the Greek and Roman
classics. His other accompUshments included general history, the
philosophy of politics in the most comprehensive acceptation, logic,
ethics, and mental philosophy. The type of his intellect was logi-
cal in the highest degree; he was, above all things, clear and pre-
cise, an enemy of every form of looseness of reasoning, and a crusher
of prevailing fallacies. This is the most notable feature in his
writings throughout. His was also an original mind. Except in a
few subjects, which had been so well elaborated by Bentham that
he was content to be little more than an expounder of Bentham's
views, he gave a fresh turn to whatever topic he took up. At a
time when social subjects were subjected almost exclusively to an
empirical handling, he insisted on bringing first principles to bear
at ever}' point; in this lay both his strength and his weakness.
His greatest literary monument is the History of J-iidia. The
materials for narrating the acquisition by England of its Indian
empire were put into shape for the fii-st time; a vast body of political
theory was brought to bear on the deUneation of the Hindu civiliza-
tion ; and the conduct of the actors in the successive stages of the
conquest and administration of India was subjected to a severe
criticism. The work itself, and the author's official connexion with
India for the last seventeen yeara of his life, effected a complete
change in the whole system of goveraing that country.
Mill played a great part as a poUticiau and political philosopher
in English affairs as well. He was, more than any other man, the
founder of what was called philosophical radicalism. His writings
on government and his personal influence among the Liberal poli-
ticians of his time determined the change of view from the French
Revolution theories of the rights of man and the absolute equality
of men to the claiming of securities for good government through
a great extension of the electoral suffrage. Under this banner it
wis that the Reform Bill was fought and won.
His work on Political Eco'wmy was intended as a text-hook of
the subject, and shows all the author's precision and lucidity. It
followed up the views of Ricardo, with whom Mill was in habitual
intimacy. It urged strongly the modem application of the prin-
ciple of population, and started the doctrine of taxing land for the
unearned uicrement of value.
By his Aiialysis of the Mind and his Fragment on Mackintosh
Mill acquired a position in the histoi7 of psychology and ethics.
Attached to tht a posteriori school, he vindicated its claims with
conspicuous ability. He took up the problem." of mind very much
after the fashion of the Scotch school, as then represented by Reid,
Stewart, and Brown, but made a new start, due in part to Hartlej-,
and still more to his own independent thinking. He caniedout the
principle of association into the analysis of the complex emotional
states, as the affections, the aesthetic emotions, and the moral
sentiment, aU which he endeavoured to resolve into pleasurable and
painful sensations. But the salient merit of the Analysis is the
constant endeavour after preci#e definition of terms and clear state-
ment of docti'ine^. The Fragmmt on Mackintosh is a severe ex-
posure of the flimsiness and misrepresentations of Mackintosh's
famous disseitation on ethical philosophy. It discusses, in a very
thorough way, the foundations of ethics from the author's point of
view of utility.
Mill's influence on the young men of his time by his conversation
has been especially celebrated. Among those that came under this
influence were some of the greatest names in the generation that
succeeded him. He had himself a very high ideal of public virtue,
which he carried out, at the risk of sacrificing all his chances of
worldly advancement, and he impressed this ideal on those that
surrounded him, — most of all on his own son, who has since eclipsed
his father in fame, if not in genius.
See J. S. Mill's Autobiography, Bain's Life of Jatnes Mill, G. S.
Bower's Hartley and James Mill. (A B. *)
MILL, John (c. 1645-1707), editor of an historically
important critical edition of the New Testament, was born
about 1645 at Shap in Westmoreland, entered Queen's
College, Oxford, as a servitor in 1661, and took his master's
degree in 1669. Soon afterwards he was chosen fellow
and tutor of his college; in 1676 he became chaplain to
the bishop of Oxford, and in 1681 he obtained the rectory
of Blechingdon, Oxfordshire, and was. made chaplain to
Charles II. From 1685 till his death he held the appoint,
ment of principal of St Edmund's Hall; and in 1704 he
was nominated by Queen Anne to a prebendal stall in
Canterbury. He died on June 23, 1707, just a fortnight
after the publication of his Greek Testament.
Mill's Novum Tcstamcntwn Grsccum, cum Icdionibus varinntibus
MSS. Exemplarium, Versionum,, Editionum SS. Paivum ct Scrip-
torum Ecclcsiastic07-um, et in. easdeni notis (Oxford, fob 1707), was
undertaken by the advice and encouragement of Fe'il, his predecessor
in the field of New Testament criticism ; it represents the labour of
thirtj* years, and is admitted to mark a great advance on all that
had previously been achieved. The text indeed is that of R.
Stephanus (1550), but the notes, besides embodying all previously
existing collections of various readings, add a vast number dcrivpil
from his own exammation of many new MSS. and Orieut.il versions
(the latter unfortunately he used only in the L.'xtiu translations).
He was the fii-st to notice, though only incidentally, the value of
the concurrence of the Latin evidence with the Codex Alcxandrinus,
the only representative of an ancient non-Westei'n Greek text then
sufficiently kno^vn ; this hint was nob lost on Beutlcy (see "Westcott
and Hort, Introduction to Xcio Testament). Mill's various readings,
numbering about thirty thousand, were attacked by AVhitby in his
Exanien as destroying the validity of the te.xt ; Antony Collins also
argued in the same sense though witli a different object. The latter
called forth a reply from Bentley (PhileUutherus Lipsicnsis). In 1710
Kuster reprinted Mill's Testament at Amsterdam with the readings
of twelve additional MSS.
MILL, John Sttjakt (1806-1873), son of James Mnj.
(q.v.), was born in London on the 20th May 1806. His
education was from first to last undertaken by his father,!
and is likely long to remain a standing subject for wonder
and discussion. Much of the wonder is no doubt due to:
his father's monstrous inversion of custom, the boy being,
set almost as soon as he could speak to work at our time-
honoured subjects of secondary and higher education. He
was taught the Greek alphabet at the age of three, and oue
of his earliest recollections, as he has recorded in his auto-
biography, was learning lists of common Greek words witm
their English meanings, written for him by his father on|
cards. By his eighth year he had gone through in the
original a great many Greek books. " Of grammar," he
says, " until some years later, I learnt no more than the
inflexions of the nouns and verbs, but after a course of
vocables proceeded at once to translation ; and I faintly
308
M i L, L,
remember going through ^sop's Fables, the first Greek
book which I read. The Anabasis, which I remember
better, was the second. I learnt no Latin until my eighth
year. At that time i had road under my father's tuition
a number of Greek proso authors, among whom I remember
the whole of Herodotus and of Xenophon's Cyropcedia and
ifemoi-ials of Socrates, some of the lives of the philosophers
by Diogenes Laertius, part of Lucian, and Isocratcs Ad
Demoniciim and Ad Nicoclem. I also rei^d, in 1813, the
first six dialogues (in the common arrangement) of Plato,
from the Euthypkron to the Theatetvs inclusive." Besides
all these Greek books, he had read a great deal of history
in English — Robertson's histories, Hume, Gibbon, Wat';bn's
Philip II. and III., Hooke's Roman History, Kollin's
Ancient History, Langhorne's Plutarch, Burnet's History
of My Oivn Times, thirty volumes of the Annual Bcgister,
Millar's Historical View of the English Government,
Mosheim's Ecclesiastical History, M'Crie's Knox, and two
histories of the Quakers.
That Mill " knew Greek " and " read Plato " before he
was eight years old is often repeated, sometimes as an
instance of amazing precocity, sometimes as an awful
example of injudicious parental forcing. The astonishment
that a child should have done so much at such an age is
probably as little grounded in reason as was ilill'S own
opininn that any child might have done the same. It is
forgotten that many thousands of persons have known
Greek before the age of eight without a knowledge of the
technicalities of Greek grammar. In presence of the fact
that Mill was never distinguished for great memory of
detail or richness of historical or literary allusion, it is a
fair conclusion that the matter of his reading at this age
was of as little service to him in after life as if he had read
the trashiest of boy's o\vn books. This is not to say that
for educational purposes his early years were wasted as in
his own and his father's opinion they generally are. But
undoubtedly the main factor in Mill's education was not
the literature put into his hands, but his constant inter-
course with the active richly stored mind and strenuous
character of his father. , If any should be tempted to
imitate the method, they should bear in mind that this
was the cardinal element of it. The tutor was of more
importance than the books. The reading of Plato's
dialogues would have been only an exercise in rough
translation if the boy had not had a Socrates with him in
living communion. The child was a constant inmate of
his father's study, and trotted by his side in his walks,
giving from jottings on slips of paper as good an account
as he could of what he had read. Ho thus learnt at an
unusually early ago by example, precept, and practice the
habit of strenuous application to difficult work. The
fact that MUl was taught thus early to take his chief
pleasure in overcoming intellectual difficulties, and to realize
the meaning of general terms, accounts for the singular
and altogether unparalleled ease which he acquired in the
treatment of political and social generalizations, not in
b:%rren abstract vagueness, but in close relation with facts.
This on the intellectual side ; and on the moral side the
child was almost from the da^vn of consciousness instructed
to regard himself as consecrated to a life of labom- for the
public good ; his ambition was kindled to follow in the
footsteps of the groat men of all ages, and at the same
time the utmost care was taken to purify that ambition
from unworthy motives.
A contemporary record of Mill's studies from eight to
thirteen is published in Dr Bain's sketch of his life. It
shows that the A'.:tobiograj>liy rather understates than
overstates the amount of work done. At the age of eight
he began Latin, Euclid, and algebra, and was appointed
schoolmaster to the younger children of the family — a
post, he hints, more serviceable to his intellect than to his
manners. His main reading was still history, but he went
through all the Latin and Greek authors commonly read
in the schools and universities, besides several that arc not
commonly read by undergraduates. Ho was not taught to
compose either in Latin or in Greek, and ho was never au
exact scholar in the academic sense ; it was for the subject-
matter that he was required to read, and by the age of
ten he could read Plato and Demosthenes with ease. His
father's History of India was published in 1818; immedi-
ately thereafter, about' the ago of twelve, John, under his
energetic direction, began a thorough study of the scholastic
logic, at the same time reading Aristotle's logical treatises
in the original In the following year he was introduced
to political economy. And there, when the pupil waa
nearly fourteen, this remarkable education terminated.
From that time he worked less immediately under his
father's eye. It was an inevitable incident of such an
education that MUl should acquire many of his father's
speculative opinions, and his father's way of defending
them. But his mind did not receive the impres" passively
and mechanically. " One of the grand objects of educa-
tion," according to tl.e elder Mill, "should be to generate
a constant and anxious concern about evidence"; and he
laboured vrith all the energy of his strong will against
allowing his son to become a parrot of his own opinions
and arguments. The duty of collecting and weighing
evidence for himself was at every turn impressed upon the
boy ; he was taught to accept no opinion upon authority ;
he was soundly rated if he could not gi-sje a reason for his
beUefs. John Stuart Mill was debberately educated as an
apostle, but it was as an apostle of reasoned truth in
human affairs, not as an apostle of any system of dogmatic
tenets. It was purposely to prevent any falling off from
this high moral standard till it should become part of his
being that his father kept the boy so closely with himself.
Much pity has been expressed over the dreary cheerless
existence that the child must have led, cut off from all
boyish amusements and companionship, working day after
day on his father's treadmill ; but a childhood and boyhood
spent in the daily enlargement of knowledge, with the
continual satisfaction of ditficulties conquered, buoyed n]>
by day-dreams of emulating the greatest of human
benefactors, need not have been an unhappy childhood,
and Mill expressly says that his was not unhappy. It
seems unhappy onlj' when wo compare it with the desires
of childhood left more to itself, and when we decline to
imagine its peculiar enjoyments aud aspirations. Mill
complains that his father often required more than could
reasonably be expected of him, but his tasks were' not bo
severe as to prevent him from growing up a healthy, hardy,
and high-spirited boy, though he was not constitutionally
robust, and his tastes and pursuits were so different from
those of other boys of the same ago.
Most of Mill's fifteenth year was spent in France in the
family of Sir Samuel Bentham. Away from his father,
ho maintained his laborious habits ; the disciiilino held.
Copious extracts from a diary kept by him at this timo
are given by Dr Bain, and show how methodically and
incessantly he read and wrote, studied botany, tackled
advanced mathematical problems, made notes on the scenery
and the people and customs of the country. On his return
in 1821 he continued his old studies with the addition of
some new ones. One of the new studios was Boman law,
which he read vdlh John Austin, his father having lialf
decided on the bar as the best jirofcssiou open to him.
Another was psychology. In 1823, (vhen he bad just
completed his seventeenth year, the notion of the l<ar as a
livelihood was abandoned, and he entered as a clerk in the
examiner's office of the India House, " with the under-
MILL
309
i
standing that he should be employed from' the beginning
in preparing drafts of despatches, and be thus trained up
as a successor to those who then filled the highest depart-
ments of the office."
Mill's work at the India Ho^ise, which was henceforth
his livelihood, did not come before the public, and those
who have scouted his political writings as the work of an
abstract philosopher, entirely unacquainted ■n-ith affairs,
have ignored the nature of his duties. From the first he
was more than a clerk, and after a short apprenticeship he
was promoted, in 1828, to the responsible position of
assistant-examiner. The duty of the so-called examiners
was to examine the letters of the agents of the Company
in India, and to draft instructions in reply. The character
of the Company's government was almost entirely depend-
ent upon their abilities as statesmen. For twenty years,
from 1S36 to 1856, Mill had charge of the Company's
relations with the native states. In the hundreds of
despatches that he wrote in this capacity, much, no doubt,
was done in accordance with established routine, but few
statesmen of his generation had a wider experience of the
responsible application of principles of government to
actual emergencies. That he said so little about this work
in the Autobiography was probably because his main con-
cern there was to expound the influences that afiected his
moral and mental development. A man of different
temperament might have found abundance of dramatic
interest in watching the personal and political changes in
so many distinct states. But Mill makes no reminiscences
of this kind, nor does he give any clue to the results of
his own initiative.
To return to his extra-oflicial activity, which received an
immense impulse about the time of his entering the India
House from what must strike a man of the world as a strange
source. The reading of Dumont's e.xposition of Bentham's
doctrines in the Traite de Legislation was an epoch in
Mill's life. It awoke in him an ambition as enthusiastic
and impassioned as a young man's first love. The
language that he uses about it in his autobiography reveals
a warmth of inner life that few people would suspect from
the record of his dry studies. When he laid do\vn the last
volume, he says, he had become a different being. It
gave unity to the detached and fragmentary component
parts of his knowledge and beliefs. "I now had opinions —
a creed, a doctrine, a philosophy — in one among the best
senses of the word, a religion, the inculcation and diffusion
of which could be made the principal outward purpose of
a life. And I had a grand conception laid before me of
changes to be effected in the condition of mankind through
that doctrine." He had been carefully bred to contemplate
work for human welfare as the ruling motive of his life ;
that motive had now received definite direction.
Many a youth has entered the world with ambition
equally high, but few have felt as Mill felt the first shock
of despair, and fewer still have rallied from that despair
with such indomitable resolution. The main secret of the
great " crisis " of his youthful life is probably to be found
in the lofty ardour of the aspirations then conceived and
shaped. For four years he worked vrith faith and hope in
his mission, and these were years of incessant propagandist
activity. The enthusiast of seventeen, burning to reorganize
human affairs so as to secure the greatest happiness of the
greatest number, set siege to the public nrind through
several approaches. He constituted a few of his youthful
friends, imbued with the principles of his new creed, into
a society which he called the " Utilitarian " Society, taking
the word, as he tells ns, from one of Gait's noveb. Two
newspapers were open to him — the Traveller, edited by a
friend of Bentham's, and the Chronicle, edited by his
lather's friend BlacL One of his first efforts was a solid
argument for freedom of discussion, in a series of letters
to the Chronicle apropos of the prosecution of Richard
Carlile. But he watched all public incidents with a
vigilant eye, and seized every passing opportunity of
exposing departures from sound principle in parliament
and courts of justice. Another outlet was opened up for
him in 1824 by the starting of the Westmimier Review,
and still another in the following year in the Parliamentary
History and Review. This year also he found a congenial
occupation in editing Bentham's Rationale of Judicial
Evidence. Into this he threw himself with zeal And all
the time, his mind full of public questions, he discussed
and argued eagerly with the ma^ny men of promise and
distinction who came to his father's house. He engaged
in set discussions at a reading society formed at Crete's
house in 1825, and in set debates at a Speculative Society
formed in the same year.
"A very disquisitive youth," was Peacock's description
of young Mill at this period, and this was probably how
the enthusiast struck most' of his outside acquaintances.
But the glow of a great ambition as well as the energy of
a piercing intellect might have been felt in his writings.
His mission was none the less arduous that he proposed to
convert the world by reason. Only the fulness of unbroken
hope could have supported his powers, if he had had a
frame of iron, under the strain of such incessant labour.
All of a sudden, a misgiving which he compares to the
Methodist's " first conviction of sin " made a rift in the
wholeness of his faith in his mission. "It was in the
autumn of 1826. I was in a dull state of nerves, such
as everybody is occasionally liable toj unsusceptible to
enjoyment or pleasurable excitement ; one of those moods
when what is pleasure at other times becomes insipid or
indifferent In this frame of mind it occurred to
me to put the question directly to myself, ' Suppose that
all your objects in life were realized, that all the changes
in institutions and opinions which you are now looking
forward to could be completely effected at this very
instant, would this be a great joy and happiness to you ! '
And an irrepressible self-consciousness distinctly answered,
' No ! ' At this my heart sank within me ; the whole
foundation on which my life was constructed fell down.
All my happiness was to have been found in the continual
pursuit of this end. The end had ceased to charm, and
how could there ever again be any interest in the means I
I seemed to have nothing left to Uve for."
The passage in his autobiography in which Mill gives
an account of this prostrating disenchantment and his
gradual release from its benumbing spell is one of the most
interesting chapters in personal history. The first break in
the gloom came, he tells us, from his reading in Marmontel's
Memoires "the passage which relates his father's death,
the distressed position of the family, and the sudden
inspiration by which he, then a mere boy, felt and made
them feel that he would be everything to them — would
supply the place of all that they had lost." Mill was
moved to tears by the narrative, and his burden grew
lighter at the thought that all feeling was not dead vrithin
him, that he was not a mere intellectual machine. This
incident, and the delight that he now began to take in
Wordsworth's " Poems founded on the Affections," gives a
clue to one of the secrets of Mill's despondency. It was
an unsatisfied longing for personal affection, for love and
friendship, of which his life hitherto had been barren.
His father seems to have been reserved, undemonstrative
even to the pitch of chilling sternness in his intercourse
with his farnily ; and among young Mill's comrades con'
tempt of feeling was almost a watchword, because it is s«
often associated with mischievous prejudice and wrong
conduct. Himself absorbed in abstract questions and pro
310
M ILL
jects of general philanthropy, he had been careless of
winning or keeping personal attachment. But it was not
till despair first seized him, as he looked back at the
poverty of the results of his work as an apostle, that Mill
began to feel the void in his affections and the need of
human sympathy. We must remember -how little when
his ambition was formed he knew of the living world
around him. He knew in terms that political and social
change must be slow ; he could whisper patience to him-
self, and say to himself that his life must be happy because
the attainment of his great object must occupy the whole
of it; but without experience he could not have been
prepared for the actual slowness of the reformer's work, or
armed against its terribly oppressive influence. Inevitably
he underrated the stolidity and strength of the forces
arrayed against him. Four years seems a long time at that
age. In 1826 Mill could look back to four years of eager
toil. What were the results 1 He had become convinced
that his comrades in the Utilitarian Society, who never
numbered more than ten, had not the stuff in them for a
world-shaking propaganda ; the society itself was dissolved;
the Parliamentary Beview was a failure ; the Westminster
did not pay its expenses ; Bentham's Judicial Evidence pro-
duced little effect on the reviewers. His own reception at
the Speculative Debating Society, where he first measured
his strength in public conflict, was calculated to produce
self-distrust. He found himself looked upon with curiosity
as a precocious phenomenon, a " made man," an intellectual
machine set to grind certain tunes. The most clear and
cogent reasoning failed to sway his audience. Great things
had been expected of this society as a means of bringing
together for close discussion the leading young men then
in public life or looking forward to it. Its first session
proved a fiasco, llie leaders that had been expected stayed
away. With these repulses to his hopes along the whole
line of his activity. Mill must also have suffered from the
nervous exhaustion that only the hope and heat of the
fight had kept him from feeling before. No wonder that
he was disheartened, began to feel defects in his father's
training, to question and analyse his own faith, to yearn
for the solace of personal affection, and to reconstitute his
scheme of life.
That in spite of this rude shock the foundations laid by
his early training remained stable appears from the facts
that all through the period of his gloom he continued
working as before, and that he considered himself bound,
once convinced that his old plan of life was insufficient, to
build up a thoroughly reasoned new plan wherewith to
give new heart and hope to his work. The new system
was much less different from the old than might be sup-
posc.l from what he says of the struggle that it cost him
to reach it. Regard for the public good was still his
religion, the ruUng motive that gave unity to his conduct.
But he now recognized that this was too vague and insub-
stantial an object to be sufficient of itself for the satisfac-
tion of a man's affections. It is a proof of the dominating
force of his father's characte'r that it cost the younger Mill
such an effort to shake off his stern creed about poetry
and personal emotion. Like Plato, the elder Mill would
have put poets under ban as ministers of prejudice and
enemies of truth. And ho often insisted on the wisdom
of rcst-ricting as much as possible the private affections,
while expanding as much as possible the public affections.
Lander's maxim of " few acquaintances, fewer friends, no
familiarities" had his cordial approval. These doctrines
the younger Mill at first took up with boyish enthusiasm
and pedantry, but it was against this part of his father's
creed that he now felt himself forced in reason to revolt.
He stood too much in awe of his father to make him the
confidant of his difficulties. He wrestled with them in
the gloomy solitude of his own mind. He was victorious -
he reached firm ground at last ; but the struggle left him
in several respects changed. He carried out of the struggle
as the fruits of victory a more catholic view of the elements
of human happiness, a delight in the poetry of nature and
the affections as well as the poetry of heroic unselfish
character and action, a disposition to study more sympa-
thetically the point of view of opponents, a more courteous
style of polemic, a hatred of sectarianism, an ambitioa
no less noble and disinterested but moderated to practical
possibilities.
In the course of the next few years Mill ■UTote compara^
tively little, but he " carried on," as he says, " a quantity
of thinking respecting a host of subjects." It was a period
of search, deliberation, germination, and striking root.
Coincident if not causally connected with the relief from
his spiritual crisis came his first consciousness of power
as " an original and independent thinker." In the dia-
lectic conversations with a small band of students at
Grote's house, he regained the self-confidence that had beeii
shaken in the larger and rougher arena of the Speculative
Debating Society. The beginning of his worlcs on logic
and political economy may be traced back to those discus-
sions, and he learnt from them, he tells us, the habit of
"never accepting half solutions of difficulties as complsta ;
never abandoning a puzzle, but again and again returning
to it until it was cleared up ; never allowing obscura
corners of a subject to remain unexplored, because they dirt
not appear important ; never thinking that he perfectly
understood any part of a subject until he understood the
whole." He learnt also an important moral lesson from
the Speculative Society, besides learning the stvong pomts
of other political and social creeds and the weak points of
Benthamism from defending it point by point against alt
comers. With all his despondency, he did not abandon
the meetings of the society after the fiasco of the firs:
session. He stood by it firmly, and in a short time had
the triumph of seeing its debates famous enough to attract
men with whom it was profitable for him to interchange
opinions, among others Maurice and Sterling. He ceased
to attend the society in 1829, but he carried away from
it the strengthening memory of failure overcome by per-
severing effort, and the important doctrinal conviction that
a true system of poUtical philosophy wai "something much
more complex and many-sided than ht had previously had
any idea of, and that its office was to supply, not a set
of model institutions, but principles from which the insti-
tutions suitable to any given circumstances might be
deduced."
The first sketch of Mill's political philosophy appeared
in a series of contributions to the Examiner in the autumn
of 1830 on "Prospects in France." He was in Paris soon
after the July Revolution, made the acquaintance of the
leading spirits among the younger men ; and in his discus-
sion of what they were doing and what they should do in
making a new constitution we find the germs of many
thoughts afterwards more fully developed in his Rejyreten-
iative Govemmeni.
Tho division of a man's life into periods must always
be a rough partition, but we may conveniently and T^^th
tolerable accuracy take those letters as marking the close
of his period of meditative search, of radication, and his
return to hopeful aspiring activity. It was characteristic
of the nature of the man that he should bo stirred to such
delight by the Revolution in France, and should labour so
earnestly to make liis countrymen understand with what
gravity and sobriety it had been effected. Their own
Reform Bill came soon after, and it is again characteristic
of Mill — at once of his enthusiasm and of his steady deter-
mination to do for humanity the work that nobody else
MILL
111
aee«ed able or willing to do — that we find him in the heat
of the struggle in 1831 writing to the Examiner a series
of letters on " The Spirit of the Age " which drew from
Carlyle the exclamation, "Here is a new mystic!" We
can easily see now what it was in these remarkable essays
that fascinated Carlyle ; it was the pervading- opinion that
in every natural state of society power must be in the
hands of the wisest. This was the condition of stability;
when power and wisdom ceased to coincide, there was a
disturbance . of the equilibrium till this coincidence was
again effected. But whether Carlyle was right in the
epithet " mystic " may be judged from the fact that Mill's
inductive logic was the direct result of his aspirations after
political stability as determined by the dominion of the
wisest. " Why is it," he asked, " that the multitude accept
implicitly the decisions of the wisest, of the specially
skilled, in physical science 1 " Because in physical science
there is all but complete agreement in opinion. " And why
this agreement 1 " Because all accept the same methods
of investigation, the same tests of truth. Is it possible
then to obtain unanimity as to- the methods of arriving at
conclusions in social and political matters, so as to secure
similar agreement of opinion among the specially skilled,
and similar general respect for their authority? The
same thought appears in a review of Herschel's Natural
Philosophy, -written about the same time. Mill remarks
that the uncertainty hanging over the very elements of
moral and social philosophy proves that the means of
arriving at the truth in those sciences are not yet properly
understood. " And whither," he adds, " can mankind so
advantageously turn, in order to learn the proper means,
and to form their minds to the proper habits, as to that
branch of knowledge in which by universal acknowledg-
ment the greatest number of truths have been ascertained,
and the greatest possible degree of certainty arrived at!"
By 1831 Mill's enthusiasm for humanity had been
thoroughly reawakened, and had taken the definite shape
of an aspiration to supply an unimpeachable method of
search for conclusions in moral and social science. From
the platform on which Carlyle and Mill met in 1831 they
travelled different roads, ^the one to preach the duty of
obedience to the wisest, the other to search for a means by
which wisdom might be acquired such as would command
respect and -win the assent of free conviction. No mystic
ever worked with warmer zeal than Mill. But his zeal
encountered a check which baffled him for several years,
and which left its mark in various inconsistencies and
incoherences in his completed system. He had been bred
by his father in a great veneration for the syllogistic logic
as an antidote against confused thinking. He attributed
to his early discipline in this logic an impatience of vague
language which in all likelihood was really fostered in hi-m
by his study of the Platonic dialogues and of Bentham, for
he always had in himself more of Plato's fertile ingenuity
in canvassing the meaning of vague terms than the school-
man's rigid consistency in the use of them. Be this as it
may, enthusiastic as he was for a new logic that might
give certainty to moral and social conclusions, MiU was no
less resolute that the new logic should stand in no
antagonism to the old. In his Westminster ireView of
Whately's Logic in 1828 (invaluable to all studeixls of the
genesis of Mill's logic) he appears, curiously enough, as an
ardent and brilUant champion of the syllogistic logic against
highfliers such as the Scotch philosophers who talk of
" superseding " it by " a supposed system of inductive
logic." His inductive logic must "supplement and not
supersede." It must be concatenated -with the syllogistic
logic, the two to be incorporated in one system. But for
several years he searched in vain for the means of con-
catsnation.
Meantime, whUe recurring again and again, as was his
custom, to this cardinal difficulty, Mill worked indefatigably
in other directions -where he saw his way clear, expatiating
over a -wide range of political, social, economical, and
philosophical questions. The working of the new order in
France, and the personalities of the leading men, had a pro-
found interest for him ; he wrote on the subject in the
Examiner. He had ceased to write for the Westminster
in 1828; but during the years 1832 and 1833 he con-
tributed many essays to Tail's Mar/azine, the Jurist, and
the Monthly Repository. In 1835 the London Review was
started, with Mill as editor ; it was amalgamated with the
Westminster in 1836, and Mill continued editor till 1840.
Much of what he -wrote then was subsequently incorporated
in his systematic works ; some of his essays were reprinted
in his first two volumes of Dissertations and Discussions
(1 859). The essays on Bentham and Coleridge constituted
the first manifesto of the new spirit which Jlill sought to
breathe into English Radicalism. Biat the reprinted papers
give no just idea of the immense range of Mill's energy at
this time. His position in the India Office, where alone
he did work enough for most men, cut him off from
entering parliament ; but he laboured hard though
ineffectually to influence the legislature from without by
combating the disposition to rest and be thankful. In
his Autobiography he admits that the attempt to form a
Radical party in parliament at that time was chimerical.
It was in 1837, on reading Wliewell's Inductive Sciences
and re-reading Herschel, that Mill at last saw his way
clear both to formulating the methods of scientific investi-
gation and joining on the new logic as a supplement to the
old. Epoch-making as his logic undoubtedly was, from
the multitude of new views opened up, from the addition
of a new wing to the rambling old building, and from the
inspiring force ivith which every dusty chamber was
searched into and illuminated. Mill did not escape all the
innumerable pitfalls of language that beset the pioneer in
such a subject. It is evident from a study of his purposes
and the books from which he started that his worst
perplexities were due to his determination to exhibit
scientific method as the complement of scholastic logic.
In his defence of the syllogism he confounds the syllogistic
forms with deductive reasoning. Every deductive reason-
ing may be thrown into the form of a syllogism, but not
every syllogism is deductive. The reasoning in several of
the syllogistic forms is not deductive at all in the sense
of involving a movement from general to particular.
Although he knew Aristotle in the original. Mill did not
recognize the fact that the syllogistic machinery was
primarily constructed for the reasoning together of terms.
As regards the word induction, Mill uses it in different
connexions to cover three or four distinguishable meanings
— induction viewed as the establishment of predications
about a general term, induction viewed as inference from
the known to the unknown, induction viewed as verifica-
tion by experiment, and induction viewed as the proof of
propositions of causation. The form of his system was
reaUy governed by the scholastic notion of induction as a
means of establishing general propositions ; the inductive
part of his system is introduced after the deductive under
this character ; while the greater portion of the substance
of what he treats of under the name of induction, and
especially the so-called exjieri mental methods, have nothing
whatever to do with the establishment of general proposi-
tions, in the technical sense of general propositions.'
But the permanent value and influence of Mill's inductive
logic is not to be measured by technical inaccuracies and
inconsistencies, to which an academic mind may easily
attach undue importance. In the technical history of the
science, ilill's Logic may be viewed as an attempt to fuse
312
]\f I L L
tlie i)ractical tests of truth set forth in Herschel's Discourse
(■11 Natural Philosophy with the theoretic views of induc-
tion propounded in Whately's Logic. But in the history
of tliought the great importance of the work is duo not so
much to its endeavour to formulate the methods of science
and lay bare the first principles on which they rest as to
its systematic application of scientific method to what he
called the moral sciences. Mill has often been criticized
as if he had pretended to teach men how to conduct their
■ investigations and how to make discoveries in the physical
sciences. His work was rather to educe from the practice
of men of science the principles on which they proceed in
testing and proving their speculations concerning cause
and effect in the physical world, and see whether the same
principles could not be applied in testing and proving
speculations concerning «ause and effect in the moral
world. What is the effect upon human character and
human happiness of given social and physical conditions —
climate, institutions, customs, laws ? How can conclusions
upon such points be proved ? These were the questions
in which Mill was interested, and the striking novelty of
his work was its endeavour to show that propositions of
cause and effect in human affairs must be proved, if they
admit of proof at all, absolute or approximate, on the
same principles with propositions of cause and effect in
the material world.
The Logic was published in 1843. In 1844 appeared
his Essays on Some Unsettled Qtiestioiis in Political
^Economy. These essays were worked out and written
many years before, and show ^lill in his first stage as a
political economist. Four out of the five essays are
elaborate and powerful solutions of perplexing technical
problems — the distribution of the gains of international
commerce, the influence of consumption on production, the
definition of productive and unproductive labour, the pre-
cise relations between profits and wages. Though Mill
appears here purely as the disciple of Ricardo, striving
after more precise statement, and reaching forward to
further consequences, we can well understand in reading
these essays, searching, luminous, large and bold in outline,
firmly wrought in detail, how about the time when he first
sketched them he began to be conscious of power as an
original and independent thinker.
That originality and independence became more con-
spicuous when he reached his second stage as a political
economist, struggling forward towards the standpoint
from which his systematic work was written. It would
seem that in his fits of despondency one of the thoughts
that sat upon him like a nightmare and marred his dreams
of human improvement was the apparently inexorable
character of economic laws, condemning thousands of
labourers to a cramped and miserable existence, and
tkousands more to semi-starvation. From this oppressive
feeling he found relief in the thought set forth in the
opening of the second book of his Political Economy — that,
while the conditions of production have the necessity of
physical laws, the distribution of what is produced among
the various classes of producers is a matter of human
arrangement, dependent upon alterable customs and
institutions. There can be little doubt that this thought,
whether or not in the clear shape that it afterwards
assumed, was the germ of all that is most distinctive in
]iis system of p^litical economy. It was as far as possible
from the rigidity of his method of exposition to fall into
the confusion of supiiosing that it was for political
economy to discuss the equity of different modes of
distribution, or the value of other objects of human
fndeavour conflicting with the i>roduction of wealth ; but
he ])ut economic inquiri'.\s cloariy in tlicir proper place as
leading to conclusions tkit were not always tiual and bind-
ing on tho practical statesman, but had to be taken with
other considerations as governing rational human action.
Besides thus putting political economy in its just correla-
tion with other parts of social science and conduct, Jlill
widened the scope of economic inquiries by discussing the
economic consequences of variotis ideal social arrangement.s,
and more especially different modes of distributing produce
between landlord, capitalist, and labourer, ilill certainly
redeemed political economy from the reproach of being a
dry science. Nobody with any interest in human improve-
ment can read his work with indifference. And he did
this without in any way disturbing the original conception
of poUtical economy as the science of cause and effect in
the production of wealth. One of his most eminent
successors, the late Professor Cairnes, thus admirably
summed up his work as a political economist : — " As he
himself used to put it, Ricardo supplied the backbone of
the science ; but it is not less certain that the limbs, the
joints, the muscular developments — all that renders
political economy a complete and organized body of
knowledge — have been the work of Mill."
While his great systematic works were in progress,
Mill wrote very little on events or books of the day. Ho
turned aside for a few months from his Political Economy,
during the winter of the Irish famine (1846-47) to
advocate the creation of peasant-proprietorships as a
remedy for distress and disorder in Ireland. He found
time also to write elaborate articles on French history and
Greek history in the Edmhurgh Ecvieio apropos of Jlichelet,
Guizot, and Grote, besides some less elaborate essays.
The Political Economy was pubhshed in 1848. Slill
could now feel that the main work he had proposed for
himself was accomplished ; but, though he wrote compara-
tively little for some years afterwards, he remained as
much as ever on the alert for opportunities of useful
influence, and pressed on with hardly diminished
enthusiasm in his search for useful truth. Among other
things, he made a more thorough study of socialist wTiters,
with the result that, though he was not converted to any
of their schemes as being immediately practicable, he
began to look upon some more equal distribution of the
produce of labour as a practicability of the remote future,
and to dwell upon the prospect of such changes in human
character as might render a stable society possible without
the institution of private property. This he has called his
third stage as a political economist, and he says that he
was helped towards it by the lady, Mrs Taylor, who became
his wife in 1851, and with whom he had lived in intimate
friendship for more than twenty years before. It is
generally supposed that he writes with a lover's extrava-
gance about this lady's powers when he compares her with
Shelley and Carlyle. But a little reflexion will show that
he wrote with his usual accuracy and sobriety wlien he
described her influence on him. He expressly says that
he owed none of his technical doctrine to her, that she
influenced only his ideals of life for the individual and for
society ; and his language about her is really only a
measure of the importance that he attached to such ideals
above any systems of reasoned truth. There is very little
propositional difference between Mill and his father ; but
it is obvious from what ho says that his inner life became
very different after he threw off his father's authority.
This new inner life was strengthened and enlarged by Mrs
Taylor. Wc must remember also that Mill in his early
years had been so strictly secluded from commonplace
sentiment that what the general world would consider
commonplace must have come to him with all the freshness
of a special revelation.
During the seven years of his married life Mill published
lean than 'a ouy other period of his career, but four of his
MILL
313
most closely reasoned and characteristic works, the Liberti/,
the Utilitarianism, the Thonr/hts on Parliamentary Reform,
and the Subjection (f Women, besides his posthumously
published essays on Nature and on the Utility of Religion,
were thought out and partly written in collaboration with
his wife. In 1856 he became head of the examiner's
office in the India House, and for two years, till the
dissolution of the Company in 1858, his official work,
never a light task, kept him fully occupied. It fell to
him as head of the office to write the defence of the
Company's government of India when the transfer of its
powers was proposed. Mill was earnestly opposed to the
transfer, and the documents in which he substantiated the
proud boast for the Company that " few governments even
under far more favourable circumstances have attempted
so much for the good of their subjects or carried so many
of their attempts to a beneficial issue," and exposed the
defects of the proposed new government, are models of
trenchant and dignified pleading. His prediction that the
Indian Secretary's council would serve as a screen and
not as a check was in the opinion of many amply verified
a few years ago.
On the dissolution ef the Company, Mill was offered a
seat in the new council, but declined. His retirement
from official work was followed almost immediately by his
vrife's death, and from this calamity he sought relief in
active literary occupation. Politics, sociology, and psycho-
logy divided as before the energies of his active mind.
One of his first cares was to publish with a touching
dedication to his wife the treatise on Liberty, which they
had wrought out together, principle by principle and
sentence by sentence. This pious duty discharged, he
turned to current politics, and published, in view of the
impending Reform Bill, a pamphlet on parliamentary
reform. The chief feature in this was an idea concerning
which he and Mrs Mill often deliberated, the necessity
of providing checks against uneducated democracy. His
fanciful suggestion of a plurality of votes, proportioned to
the elector's degree of education, was avowedly put forward
only as an ideal ; he admitted that no authentic test of
education could for the present be found. An anonymous
Conservative caught at the scheme in another pamphlet,
proposing income as a test. Soon after. Mill supported
in Eraser's, still with the same object, Jlr Hare's scheme
for the representation of minorities. In the autumn .of
the same year he turned to psychology, reviewing Mr
Bain's works in the Edinburgh Review.
In this way the indefatigable thinker worxed on, throw-
ing himself by turns into the various lines along which he
saw prospects of fulfilling his mission as an apostle of pro-
gress. In his Representative Government (1860) he systema-
tized opinions already put forward in many casual articles
and essays. His Utilitarianism (published in Eraser's in
1861) was a closely reasoned systematic attempt to answer
objections to his ethical theory and remove misconceptions
of it. As the inventor of the term Utilitarianism, he was
entitled to define its meaning ; and he was especially
anxious to make it clear that he included in utility the
pleasures of the imagination and the gratification of the
higher emotions, and to show how powerfully the good of
mankind as a motive appealed to the imagination. His
treatise on the Subjection of Women, in its ruling intention
a protest against the abuse of power, was Mill's next work,
though it was not published till 18G9. His Examination
of Hamilton's P/ii!osop/iy, published in 1865, had engaged
a large share of his time for three years before. When it
irst occurred to him that a criticism of the chief of our
native intuitional psychologists would cause a wholesome
stir and serve enlightenment, he thought only of an article
BUth as he \vrote about Austin's Jurisprudence or Grote's
16—13*
Plato. But he soon found that the subject required a book,
and a book appeared which certainly answered the purpose
of rousing the sleepy realms of philosophy and theology.
AVhile mainly occupied in those years with philosophical
studies. Mill did not remit his interest in current politics.
He made his voice heard on the contest in America in
1862, taking the side of the North — then very unpopular
in London — and using all his strength to explain what has
since been universally recognized as the issue really at
stake in the struggle, the abolition of slavery. It waa
characteristic of the closeness with which he watched
current events, and of his zeal in the cause of " lucidity,"
that, when the Reader, an organ of science and unpartisar.
opinion, fell into difficulties in ISO'S, Mill joined with some
distinguished men of science auf* letters in an effort to keep
it afloat. He supplied part of the money for carrying it
on, contributed several articles, and assisted the editor,
Mr Fraser Rae, with his advice. The effort was vain,
though such men as Herbert Spencer, Huxley, TyndaU,
Cairnes, Mark Pattison, F. Harrison, Sir Frederick Pollock,
and Lockyer were among the contributors.
In 1865 a new channel was opened to his influence.
He was requested to stand for "Westminster, and agreed
on conditions strictly in accordance with his principles of
parliamentafy election. He would not canvass, nor pay
agents to canvass for him, nor would he engage to attend
to the local business of the constituency. He was with,
difficulty persuaded even to address a meeting of the
electors. The story of this remarkable election has been
told by Mr James Beal, one of the most active supporters
of Mill's candidature. In parliament he adhered to his
lifelong principle of doing only work that needed to bs
done, and that nobody else seemed equally able or willing
to do. It may have been a consciousness of this fact
which prompted a remark made by the Speaker that Mill's
presence in parliament elevated the tone of debate. Ths
impression made by him in parliament is in some danger
of being forgotten, because he was not instrumental in
carrying any great measure that might serve as an abiding
memorial. But, although in one of his first speeches
against the suspension of the Habeas Corpus Act in Ireland
he was very unfavourably received. Mill thoroughly
succeeded in what is called " gaining the ear of the House."
The only speech made by him during his three years in
parliament that was listened to with impatience was,
curiously enough, his speech in favour of counteracting
democracy by providing for the representation of minorities.
His attack on the conduct of General Eyre in Jamaica
was listened to, but with repugnance by the majority,
although his action in this matter in and out of parliament
was far from being ineffectual. He took an active part in
the debates on Jilr Disraeli's Reform Bill, and helped to
extort from the Government several useful modifications
of the Bill for the Prevention of Corrupt Practices. The
reform of land tenure in Ireland, the representation of
women, the reduction of the national debt, the reform of
London government, the abrogation of the declaration of
Paris, were among the topics on which he spoke with
marked effect. He took occasion more than once to
enforce what he had often advocated in writing, England's
duty to intervene in Continental politics in support of the
cause of freedom. As a speaker Mill was somewhat
hesitating, pausing occasionally as if to recover the thread
of his argument, but he showed great readiness in extem-
poraneous debate. Viewed as a candidate for ministerial
office, he might be regarded as a failure in parliament, but
there can be no doubt that his career there greatly extended
his influence.
Mill's subscription to the election expenses of Mr
Bradlaugh, and his attitude towards Governor Eyre, are
:u
M I L — M I L
f,3nerally regarded as the main causes of his defeat in the
general election of 1868. But, as he suggests himself, his
studied advocacy of unfamiliar projects of reform had made
him unpopular with " moderate Liberals." WTien he was
first elected on a sudden impulse of enthusiasm, extremely
little was known about him by the bulk of the electorate;
and his writing about checks against democracy had pre-
pared many for a more conservative attitude on questions
of practical politics. He retired with a sense of relief to
his cottage and his literary life at Avignon. His parlia-
mentary duties and the quantity of correspondence brought
upon him by increased publicity had absorbed nearly the
whole of his time. The scanty leisure of his first recess
had been devoted to writing his St Andrews rectorial
address on higher education and to answering attacks on
his criticism of Hamilton ; of the second, to annotating, in
conjunction with Mr Bain and Mr Findlater, his father's
Analysis of the Mind. But now he could look forward to
a literary life pure and simple, and his letters show how
much he enjoyed the change. His little cottage was filled
■with books and newspapers ; the beautiful country round
it furnished him with a variety of walks ; he read, wrote,
discussed, walked, botanized. His step-daughter, Miss
Taylor, his constant companion after his wife's death,
"architect and master-mason all in one," carried out
various improvements in their quiet home for the philo-
sopher's comfort. "Helen," he wrote to Mr Thornton,
" has carried out her long-cherished scheme (about which
she tells me she consulted you) of a ' vibratory ' for me,
and has made a pleasant covered walk, some 30 feet long,
where I can vibrate in cold or rainy weather. The
terrace, you must know, as it goes round two sides of the
house, has got itself dubbed the ' semi-circumgyratory.'
In addition to this Helen ha-s built me a herbarium, a
little room fitted up with closets for my plants, shelves
for my botanical books, and a great table whereon to
manipulate them all. Thu.5, you see, with my herbarium,
my vibratory, and my semi-circumgyratory, I am in clover ;
and you may imagine with what scorn I think of the
House of Commons, which, comfortable club as it is
said to be, could offer me none of these comforts, or, more
perfectly speaking, these necessaries of life;" Mill was an
enthusiastic botanist all his life long, and a frequent con-
tributor of notes and short papers to the Phytologist. One
of the things that he looked forward to during his last
journey to Avignon was seeing the spring flowers and
completing a flora of the locality. His delight in scenery
frequently appears in letters written to '^•s friends during
his summer and autumn tours.
No recluse ever had a more soothing retreat than Mill s
Avignon cottage, but to the last he did not relax his
laborious habits nor his ardent outlook on human affairs.
The essays in the fourth volume of his Dissertaiioiis — on
endowments, on laud, on labour, on metaphysical and
psychological questions — were written for the Fortnightly
Jieiriiiw at intervals after his short parliamentary career.
One of his first tasks was to seud his treatise on the
Subjection of Women through the press. The essay on
Theism was written soon after. The last public work in
which he engaged was the starting of the Land Tenure
Beforra Association. The interception by the state of the
unearned increment, and the promotion of co-operative
agriculture, were the most striking features in his pro-
graram^e. He wrote in the /Examiner and made a public
speech in favour of the association a few months before
lus death. The secret of the ardour with which he took
up this question probably was his conviction that a great
struggle was impending in Europe between labour and
capital He regarded his pn-jcrt as a timely coiuprouiisu.
ilill died at Avignon on the bth of May 1873.
Witliin the limits of this nrticle it is impossible to attempt t
criticism of Mill's conclujiioiis ia so many ff&lds of research^ one
must be content with trying to indicate the purpose and the spirit
of his work. Perhaps we still stand too near to judge without biaa;
some years hence men will be better able- to say whether he made
sciolism less reckless or brought mankind appreciably nearer that
dominion of the wisest which was the remote goal of hie endeavour.
It will be long before humanity finds a nobler example of the
searcher after the best means of social improvement. He sought
after clear iJeris with the ardour of a mystic, the patience and
laborious industry of a man of science; he encountered opponents
with a generosity and a coHrtesy worthy of &uy prntx chevalicT of
mediiEval romance, while he was not inferior to that ideal in the
vigour of his blows against injustice. As regards his influence, it
has been well said that "no calculus can integrate the innumerablu
pulses of knowledge and of thought that he has made to vibrato in
the minds of his generation." He quickened thought upon every
problem that he toucJied. Any estimate of Mill's service to political
or philosophical thought at this moment ia liable to be injuri-
ously affected by the temporary discredit into which some of his doc-
trines have fallen. He was not infallible; he made no'claim to dog-
matic authority. But in criticism of detail, according to our present
light, we may easily blind ourselves to the greatness of the work
thai Mill accomplished in the development of opinion. (W. M.)
MILLAU, or Milhau, capital of an arrondissement in
the department of Ave}Ton, France, is situated on the left
bank of the Tarn, half a mile below the point at which
that river is joined by the Dourbie, and 48 miles to the
south-east of Rodez, on the Rodez and MontpeUier 'line.
Itself 1210 feet above the level of the sea, it is overlooked
by hills covered with vineyards and fruit trees or by bare and
scarped rocks. The streets of ilillau are narrow, and some
of the houses of great antiqtiity, but the town is surrounded
by spacious boulevards. On two sides the Place d'Armes
is adorned by stone columns supporting galleries of wood;
the only buildings of special interest are the Romanesque
church of Notre Dame, and the belfry of the old h6tel de
vUle. The principal industry is ths maii"*'"^ture of gloves,
but various branches of the leather manufacture are also
carried on. The chief articles of commerce are wool (both
raw and prepared), Roquefort cheese, wine, almonds, and
live stock. The population in 1881 was 16,628.
The viscounts of Millau are mentioned as early as the 10th
century; in the 16th it became one of the leading strongholds of
the Reformed party in the south of France. Ita industry suQ'ered
severely by the revocation of the edict of Nantes.
JIILLENNIUM. In the history of Christianity three
main forces are found to have acted as auxiliaries of the
gospel. They have elicited the ardent enthusiasm of many
whom the bare preaching of the gospel would never have
made decided converts. These are (1) a belief in the
speedy return of Christ and in His glorious reign on earth;
(2) mystical contemplation, which regards heavenly bless-
ings as a possible possession in the present life; and (3)
faith in a divine predestination of some to salvation and
others to perdition. Each of these forces has at particular
times proved too strong for church authority and burst the
embankments with which the chiu-ch had at once narrowed
and protected Christian life and thought. They have pro-
duced ecclesiastical, social, and political con'snilsions, where
the elemental force of religious conviction has destroyed
all organization, whether of church or of state. They have
released from its fetters the free spirit of Christianity,
though often enough they have associated with it a
fanaticism more damaging to the gosoel than the temporiz-
ing ))olicy of the hierarcliy
First in point of time came the faith in the nearness of
Christ's second advent and the establishing of His reign of
glory on the earth. Indeed it appears so early that it
might be questioned whether it ought not to bo regarded
as an essential part of the Christian religion. That
question, however, will scarcely be answered in the affirma-
tive. The ideas of the Sermon on the Mount, or the
pregnant thoughts of the Pauline theology, are inde[)endent
of the expectation that the kingdom of glory will shortly
MILLENNIUM
315
be established. On the other hand, it must be admitted
that this expectation was a prominent feature in the earliest
proclamation of the gospel, and luaterially contributed to
its success. If the primitive churches had been under the
necessity of framing a "Confession of Faith," it would
certainly have embraced those pictures by means of which
the near future was distinctly realized. But then these
pictures and dreams and hopes were just the things that
made systematized doctrine impossible ; it is possible^ to
formulate the mythological ideas, but not the shifting
imagery of the imngination.
In the anticipations of the future prevalent amongst the
early Christians (c. 50-150) it is necessary to distinguish
a fixed and a fluctuating element. The former includes
(1) the notion that a last terrible battle with the enemies
of God was impending; (2) the faith in the speedy return
of Christ ; (3) the conviction that Christ will judge all
men, and (4) will set up a kingdom of glory on earth.
To the latter belong views of the Antichrist, of the heathen
world-power, of the place, extent, and duration of the
earthly kingdom of Christ, &c. These remained in a state
of solution ; they were modified from day to day, partly
because of the changing circumstances of the present by
which forecasts of the future were regulated, partly because
the indications — real or supposed — of the ancient prophets
always admitted of new combinations and constructions.
But even here certain positions were agreed on in large
sections of Christendom. Amongst these was the expecta-
tion that the future kingdom of Christ on earth should
have a fixed duration, — according to the most prevalent
opinion, a duration of one thousand years. From this fact
the whole ancient Christian eschatology was known in
later times as "chiliasm," — a name which is not strictly
accurate, since the doctrine of the millennium was only one
feature in its scheme of the future.
1. This idea that the Messianic kingdom of the future
on earth should have a definite duration has — like the
whole eschatology of the primitive church — its roots in the
^e^-ish apocalyptic literature, where it appears at a com-
paratively late period. At first it was assumed that the
Messianic kingdom in Palestine would last for ever (so the
prophets ; cf. Jerem. xxiv. 6 ; Ezek. xxxvii. 25 ; Joel iv.
20 ; Daniel vi. 27 ; Sibyll. iii. 49 sy., 766 ; Psalt. Salom.
xvii. 4; Enoch Ixii. 14), and this seems always to have
been the most widely accepted view (John xii. 34). But
from a comparison of prophetic passages of the Old Testa-
ment learned apocalyptic writers came to the conclusion
that a distinction must be drawn between the earthly
appearance of the Messiah and the appearance of God
Himself amongst His people and in the Gentile world for
the final judgment. As a necessary consequence, a limited
period had to be assigned to the Messianic kingdom. It
is not altogether improbable that the mysterious references
to the sufferings of the Messiah had also an influence on
some minds. This, however, is doubtful. It is certain at
all events that the whole conception marks the beginning
of the dissolution of realistic and sensuous views of the
future. The age was too advanced to regard the earthly
Messianic kingdom as the end. There was an effort to
find a place among the hopes of the futiu-e for those more
spiritual and universal anticipations, according to which
eternal and heavenly blessedness will be the portion of the
faithfxJ, this earth and heaven will pass away, and God
will be all in all. As to the period to be assigned to this
earthly kingdom, no agreement was ever reached in
Judaism, any more than in the detailed descriptions of its
J9y8 and pleasures. According to the Apocalyjise of Baruch
(xl. 3) this kingdom will last "donee finiatur mundus
.'ATnjptionis." In the Book of Enoch (xci. 12) "a week"
is specified, iu the Apocalypse of Ezra (vii. 28 sq.) four
hundred years. This figure, corresponding to the four
hundred years of Egyjjtian bondage, occurs also in the
Talmud (Sanhedrin 99<t). But this is the only passage;
the Talmud has no fixed doctrine on the point. The
view most frequently expressed there (see Von Otto in
HilgenfehVs Zdlschrift, 1877, p. 527 «<?.) is that tho
Messianic kingdom will last for one thousand (some !.aid
two thousand) years. " In six days God created the
world, on the seventh He rested. But a day oi God is
equal to a thousand years (Ps. xc. 4). Henco the world
will last for six thousand years of toil and labour ; then
will come one thousand years of Sabbath rest for the iieople
of God in the kingdom of the Messiah." This idea must
have already been very common in the first century before
Christ. The combination of Gen. i., Dan. ix., and Ps. xc.
4 was peculiarly fascinating.
2. Jesus Himself speaks of only one return of the Son
of Man — His return to judgment. In speaking of it, and
of the glorious kingdom He is to introduce, He makes use
of apocalyptic images (Matt. viii. 11, xxvi. 29 ; Luke xxii.
16; Matt. xix. 28); but nowhere in the discourses of
Jesus is there a hint of a limited duration of the ilessianic
kingdom. The apostolic epistles are equally free from
any trace of chiliasm (neither 1 Cor. xv. 23 sq. nor 1 Thess.
iv. 16 sq. points in tliis direction). In the Apooxlypse of
John, however, it occurs in tlie following shape (chap. xx.).
After Christ has appeared from heaven in the guise of a
warrior, and vanqiiished the antichristian world-power,
the wisdom of the world, and the devil, those who have
remained steadfast in the time of the last catastrophe, and
have given up their lives for their faith, shall be raised un
and shall reign with Christ on tliis earth as a royal priest-
hood for one thousand years. At the end of this time Satan
is to be let loose again for a short season ; he will prepare
a new onslaught, but God will miraculously destroy him
and his hosts. Then will follow the general resurrection
of the dead, the last judgment, and the creation of new
heavens and a new earth. That all believers will have a
share in the first resurrection and in the ilessianic
kingdom is an idea of which John knows nothing. The
earthly kingdom of Christ is reserved for those who have
endured the most terrible tribulation, who have withstood
the supreme effort of the world-power, — that is, for those
who are actually members of the church of the last days.
The Jewish expectation is thus considerably curtailed in
the hands of John, as it is also shorn of its sensual
attractions. " Blessed and holy is he that hath part in the
first resurrection ; on such the second death hath no power;
but they shall be priests of God and of Christ, and shall
reign with Him a thousand years." More than this John
does not say. But other ancient Christian authors were
not so cautious. Accepting the Jewish apocalypses as
sacred books of venerable antiquity, they read them eagerly,
and transferred their contents bodily to Christianity. Nay
more, the Gentile Christians took possession of them,
and just iu proportion as they were neglected by the
Jews — who, after the war of Bar-Cochba, became indifi'er-
ent to the Messianic hope and hardened themselves once
more in devotion to the law — they were naturalized in the
Christian communities. The result was that these books
became " Christian " documents ; it is entirely to Christian,
not to Je-wish, tradition that we owe their preservation.
The Jewish expectations are adopted, for example, by
Papias, by the writer of the epistle of Barnabas, and by
Justin. Papias actually confounds expressions of Jesus
with verses from the Apocalypse of Baruch, referring to
the amazing fertility of the days of the Jlessianic kingdom
(Papias in Iren. v. 33). Barnabas {Ep., 15) give-s us the
Jewish theory (from Gen. i. and Ps. xc. 4) tliat the
present condition of the world is to last six thousand yeam
316
MILLENNIUM
from the creation, that at the beginning of the Sabbath
^'the seventh millennium) the Son of God appears, to put
in end to the time of "the unjust one," to judge the ungodly
ind renew the earth. But he does not indulge, like Papias,
in sensuous descriptions of this seventh millennium; to
Barnabas it is a time> of rest, of sinlessness, and of a holy
peace. It is not the end, however; it is followed by an
eighth day of eternal duration, — "the beginning of another
world." So that in the view of Barnabas the Messianic
reign still belongs to oStos o aluiv. Justin (Dial., 80)
speaks of chiliasm as a necessary part of complete
orthodoxy, although he knows Christians who do not
accept it. He believes, with the Jews, in a restoration
and extension of the city of Jerusalem; ha assumes that
this city will be the seat of the Messianic kingdom, and
he_ takes it as a matter of course that there all believers
(here he is at one with Barnabas) along with patriarchs
and prophets will enjoy perfect felicity for one thousand
years. In fact he reads this view into tlie Apocalypse of
John, which he understands to mean that before the
general resurrection all believers are to rule for a time
(vith Christ on earth. That a philosopher like Justin,
with a bias towards an Hellenic construction of the Christian
religion, should nevertheless have accepted its chiliastio
elements is the strongest proof that these enthusiastic
expectations were inseparably bound up with the Christian
I'aith down to the middle of the 2d century. And another
proof is found in the fact that even a speculative Jewish
Christian like Ccrinthus not only did not renounce the
chiliastic hope, but pictured the future kingdom of Christ
as a kingdom of sensual pleasures, of eating and drinking
and marriage festivities (Euseb., //. E., iii. 28, vii. 25).
3. After the middle of the 2d century these ex-
pectations were gradually thrust into the background.
They would never have died out, however, had not
circumstances altered, and a new mental attitude been
taken up. The spirit of philosophical and theological
speculation and of ethical reflexion, which began to spread
through the churches, did not know what to make of the
old hopes of the future. To a new generation they seemed
paltry, earthly, and fantastic, and far-seeing men had good
reason to regard them as a source of political danger. But
more than this, these wild dreams about the glorious king-
«(oin of Christ began to disturb the organization which the
churches had seen fit to introduce. In the interests of
self-preservation against the world, the state, and the
heretics, the Christian communities had formed themselves
into compact societies with a definite creed and constitu-
tion, and they felt that their existence was threatened by
the white heat of religious subjectivity. So early as the
year 170, a church party in Asia Minor — the so-called
yVlogi — rejected the whole body of apocalyptic writings
and denounced the Apocalypse of John as a book of fables.
All the more powerful was the reaction. In the so-called
Montanistic controversy (c. 160-220) one of the principal
issues involved was the continuance of the chiliastic
expectations in the churches. The Montanists of Asia
Minor defended them in their integrity, with one slight
modification : they announced that Pepuza, the city of
Jlontanus, would be the site of the New Jerusalem and
the millennial kingdom. Modifications of -this kind,
which have often apjiearcd in later times in connexion
with the revival of millcnnarianism, are a striking evidence
of the tendency of every sect to regard its owni little
membership as the centre of the world and its fortunes as
the kernel of universal history. After the Montanistic
controver.sy, chiliastio • views were more and more
discredited in the Greek Church ; they were, in fact,
stigmatized as "Jewish" and consequently "heretical."
It waa the Alexandrian tlieologj- that superseded them;
that is to say, Neo-Platonio mysticism triumphed over
the early Christian hope of the future, first among the
" cultured," and then, when the theology of tlie " cultured "
had taken the faith of the " uncultured " under its protec-
tion, amongst the latter also. About the year 2C0 an
Egyptian bishop, Nepos, in a_ treatise called t\ry;^os
dW-qyvp'TTuiv, endeavoured to overthrow the Origenistic
theology and vindicate chiliasm by exegetical methods.
Several congregations took his part ; but ultimately
Dionysius, bishop of Alexandria, succeeded in healing
the schism and asserting the allegorical interpretation of
the prophets as the only legitimate exegesis. During this
controversy Dionysius became convinced that the victory
of mystical theology over " Jewish " chiliasm would never
be secure so long as the Apocalypse of John passed for
an apostolic writing and kept its place among the
homologoumena of the canon. He accordingly raised the
question of the apostolic origin of the Apocal}'pse; and by
reviving old difficulties, with ingenious argumenta of his
own, he carried his point. At the time of Eusebius the
Greek. Church was .saturated ■(vith prejudice against the
book and with doubts as to its canouicity. In the course
of the 4th century it was removed from the Greek
canon, and thus the troublesome foundation on which
chiliasm might have continued to build was got rid of.
The attempts of Jlethodius of Tyre at the beginning of
the 4th centurj- and Apolhnarius of Laodicea about
360 to defend chiliasm and assail the theology of Origen
had no result. For many centuries the Greek Church kept
the Johannine Apocalypse out of its canon, and consequently
chiliasm remained in its grave. It was considered a
sufhcicnt safeguard against the spirituaHzing cschatology
of Origen and his school to have rescued the main doctrines
of the creed and the regula fidei (the visible advent of
Christ ; eternal misery and hell-fire for the wicked).
Anything beyond this was held to be Jewish. It was
only the chronologists and historians of the church who,
foUo\ving Juhus Africanus, made use of apocalyi^tic
numbers in their calculations, while court theologians like
Eusebius entertained the imperial table with discussions as
to whether the dining-hall of the emperor — the second
David and Solomon, the beloved of God — might not be the
Kew Jerusalem of John's Apocalj-pse. Eusebius was not
the first who dabbled in such speculations. Dionysius of
Alexandria had already referred a Messianic prediction of
the Old Testament to the emperor Gallienus. But
mysticism and political serviUty between them gave the
death-blow to chiUasm in the Greek Church. It never
again obtained a footing there ; for, although, late in the
Middle Ages, the Book of Revelation — by what means we
cannot tell — did recover its authority, the church was by
that time so hopelessly trammelled by a magical cultus as
to be incapable of fresh developments. Li the Semitic
churches of the East (the SjTian, Arabian, and .■Ethiopian),
and in that of Armenia, the apocal}q)tic literature was
preserved much longer than in the Greek Church. They
were very conservative of ancient traditions in general, and
hence chiUasm survived amongst them to a later date than
in Alexandria or Constantinople. It is to these churches
that we are mainly indebted for the extensive remains of
the old apocalyptic literature which we now possess. From
remote cloisters of the East Europe has recovered within
the last forty years many works of this kind which once
enjoyed the highest repute throughout Christendom.
i. But the AVcstern Church was also more conservative
than the Greek. Her theologians had, to begin with, little
turn for mystical speculation ; their tendency was rather
to reduce the gospel to a system of morals. Now for
the moralists chiliasm had a special significance as the one
distinguishing feature of the gospel, and the only thing
MILLENNIUM
317
that gave a specifically Cliristian cliaracter to their system.
This, however, holds good o£ the "Western theologians only
after the middle of the 3d century. The earlier fathers,
Irenaeus, Hippolytus, TertuUian, hoUeved in chihasm
simply because it was a part of the tradition of the church
and becau.se Marcion and the Gnostics would have nothing
to do with it. Irenxus (v. 2S, 29) has the same conception
of the millennial kingdom as PKarnabas and Papias, and
appeals in support of it to the testimony of disciples of the
apostles. Hippolytus, although an opponent of Montanism,
was nevertheless a thorough-going millennarian (see his
book De Aidichristo). Tertulhan {cf. especially Adv.
Marcion., 3) aimed at a more spiritual conception of the
millennial blessings than Papias had, but he still adhered,
especially in his Montanistic period, to all the ancient
anticipations. It is the same all through the 3d and 4th
centuries with those Latin theologians who escaped the
influence of Greek speculation. Commodian, Victorinus
Pettavensis, Lactantius, and Sulpicius Severus were all
pronounced miUennarians, hokUng by the .very details of
the primitive Christian expectations. They still beheve,
as John did, in the return of Nero as the Antichrist ; they
still expect that after the first resurrection Christ will reign
with His saints " in the flesh " for a thousand years. Once,
but only once (in the CJpspel of Nicodemus), the time is
reduced to five hundred years. Victorinus wrote a
commentary on the Apocalypse of John ; and all these
theologians, especially Lactantius, were diligent students
of the ancient Sibylline oracles of Jewish and Christian
origin, and treated them as divine revelations. As to the
canonicity . and apostohc authorship of the Johannine
Apocalypse no doubts were ever entertained in the West ;
indeed an Apocalypse of Peter was still retained in the
canon in the 3d century. That of Ezra, in its Latin
translation, must have been all but a canonical book, —
the numbers of extant manuscripts of the so-called 4 Ezra
being incredibly great, while several of them are found
in copies of the Latin Bible at the beginning of the 16th
century. The Apocalypse of Hermas was much read till
far through the Middle Ages, and has also kept its place
in some Bibles. The apocalyptic " Testamenta duodecim
Patriarcharum " was a favourite reading-book ; and Latin
versions of ancient apocaljijses are being continually
brought to light from Western libraries {e.g., the Assumpiio
Mosis, the Ascetisio Jesajee, ifcc). All these facts show
how \-igorously the early hopes of the future maintained
themselves in the West. In the hands of moralistic theo-
logians, like Lactantius, they certainly assume a somewhat
grotesque form, but the fact that these men clung to them
is the clearest evidence that in the West millennarianism
was still a point of " orthodo.xy " in the 4th century.
This state of matters, however, gradually disappeared
after the end of the 4th century. The change was brought
about by two causes, — first, Greek theology, which reached
the West chiefly through Jerome, Rufinus, and Ambrose,
and, second, the new idea of the church wrought out by
Augustine on the basis of the altered political situation of
the church. Jerome, the pupil of the Greeks, feels him-
self already emancipated from "opiniones Judaicas"; he
ridicules the old anticipations ; and, though he does not
venture to reject them, he and the other disciples of the
Greeks did a great deal to rob them of their vitality. At
the same time the influence of Greek theology was by no
means so great in the West that this of itself could have
suppressed chiliastic views. It was reserved for Augustine
to give a direction to Western theology which carried it
• clear of millennarianism. He himself had at one time
believed in it ; he too had looked forward to the holy
Sabbath which was to be celebrated by Christ and His
people on earth. But the signs of the times pointed to a
different prospect. Without any miraculous interposition
of God, not only was Christianity victorious on earth, but
the church had attained a position of supremacy. The
old Roman empire was tottering to its fall; the church
stood fast, ready to step into its inheritance. It was not
simply that the world-power, the enemy of Christ, had
been vanquished ; the fact was that it had gradually
abdicated its political functions in favour of the church.
Under these circumstances Augustine was led, in hi.s con-
troversy with the Donatists and as an apologist, to idealize
the poUtical side of the catholic church, — to grasp and
elaborate the idea that the church is the kingdom of Chrisi
and the city of God. Others before him may have taken
the same view, and he on the other hand never forgot that
true blessedness belongs to the future ; but still he was the
first who ventured to teach' that the catholic church, in its
empirical form, was the kingdom of Christ, that the
millennial kingdom had com.menced with the appearing of
Christ, and was therefore an accomplished fact. By this
doctrine of Augustine's, the old millennarianism, though not
completely e.Ttirpated, was at least banished from the realm
of dogmatic. For the oSicial theology of the church it
very soon became a thing of the past ; certain elements of
it were even branded as heretical. It still hved on, how-
ever, in the lower strata of Christian society ; and in
certain undercurrents of tradition it was transmitted from
century to century. At various periods in the history of
the Middle Ages we encounter sudden outbreaks of
miUennarianism, sometimes as the tenet of a small sect,
sometimes as a ifar-reaching movement. And, since it had
been suppressed, not, as in the East, by mystical specula-
tion, its mightiest antagonist, but by the pcUtical church
of the hierarchy, we find that wherever chiLiasm appears
in the Middle Ages it makes common cause with all
enemies of the secularized church. It strengthened the
hands of church democracy ; it formed an alHance mth
the pure souls who held up to the church the ideal of
apostolic poverty ; it tuiited itself for a time even with
mysticism in a common opposition to the supremacy of the
church ; nay, it lent the strength of its convictions to the
support of states and princes in their efforts to break the
political power of the church. It is sufficient to recall the
well-known names of Joachim of Floris, of all the numerous
Franciscan spiritualists, of the leading sectaries from the
13th to the 15th century who assailed the papacy and
the secularism of the church, — above all, the name of
Occam. In these men the millennarianism of the ancient
church came to life again ; and in the revolutionary move-
ments of the 15th and 16th centuries — especially in the
Anabaptist movements — it appears with all its old uncom-
promising energy. If the church, and not the state, was
regarded as Babylon, and the pope declared to be the
Antichrist, these were legitimate inferences from the
ancient traditions and the actual position of the church.
But, of course, the new chihasm was not in every respect
identical with the old. It could not hold its ground
without admitting certain innovations. The " everlasting
gospel " of Joachim of Floris was a different thing from
the announcement of Chiist's glorious return in the clouds
of heaven ; the " age of the spirit " which mystics and
spirituahsts expected contained traits which must be
characterized as " modern " ; and the " kingdom " of the
Anabaptists in Munster was a Satanic caricature of that
kingdom m which the Christians of the 2d century looked
for a peaceful Sabbath rest. Only we must not form om-
ideas of the great apocalyptic and chihastic movement of
the first decades of the 16th century from the rabble in
Miinster. There were pure evangelical forces at work in
it ; and many Anabaptists need not shun comparison with
. the Christians of the apostolic and postrapostolic ages.
318
M T L — ]\I I L
/riic German and Swiss Reforrners also believed that the
end of tlic world was near, but they had different aims in
view from those of the Anabaptists. It was not from
poverty and apocalypticism that they hoped for a reforma-
tion of the church. In contrast to the fanatics, after a
brief hesitation they threw miUennarianism overboard,
and along with it all other "opiniones Judaica;." They
took up the same ground in this respect which the
Roman Catholic Church had occupied since the time of
Augustine. How miUennarianism nevertheless found it:i
way, with the help of apocalyptic mysticism and Anabaptist
influences, into the chiu-ches of the Reformation, chiefly
among the Reformed sects, but afterwards also in the
Lutheran Church, how it became incorporated with
Pictissn, how in recent times an exceedingly mild tyjie of
" academic " chiUasm has been developed from a belief in
the verbal inspiration of the Bible, how finally new sects
are still springing up here and there with apocalyptic and
chiliastic expectations, — these are matters which cannot be
fully entered upon here. But one remark ought to be
made in conclusion. A genuine and Living revival of
chiliastic hopes is always a sign that the church at large
has become secularized to such a degree that tender
consciences can no longer feel sure of their faith within
her. In this sense all chiliastic phenomena in the history
of the church demand respectful attention. But when
attempts are made to find room for miliennariani.sm in a
dogmatic system, it must always assume a form in which
it would be utterly unrecognizable to the millennarians
of the ancient church, who, just because they were
millennarians, despised dogmatic, in the sense of philo-
sophical theology. The claims of chiliasm are sufficiently
met by the acknowledgmeut that in former times it was
associated — to all appearance inseparably associated —
with the gospel itself. Those who try to remodel it,
so as to conserve its " elements of truth," put contempt
on it while they destroy it; for it was in its day the
most uncompromising enemy of all remodelling, and it
'can only exist along with the tinsophisticated faith of the
early Christians.
Cf. Srhiiror, Lchrbiirh iter Kcuiestatiuntlichcn ZcUt/cschicliU, 187J,
§§ 2S, 29 ; Corroili, Krilhclic Gcschkhic iles aiiliasmus, 1781. A
thoiongli history of diiliasDi lias not yet appeared. (A, HA.)
^ MILLER, Hugh (1802-1856), eminent in science and
literature, and one of the most remarkable among self-
taught men of genius, was born at Cromarty, on the north-
east coast of Scotland, on the 10th of October 1S02. His
father, a sagacious and strong-willed seaman, who earned a
livelihood by sailing his own sloop, perished at sea when
Hugh was five years old. His mother looked much, iu
the upbringing of her son, to her two brothers, James and
Alexander Wright, the one a saddler, the other a carpenter.
Scrupulous integrity, sincere religion, unflagging industry,
and resolute contentment were the lessons which these
men, not so much by precept as by example, impressed
upon the boy. But young Miller had inherited from his
father a strong individuality and obstinate force of will,
and began at a very early age to take a line of his own.
The enchantment of open air and freedom^the irresistible
charm of mother nature on the hill and by the sea — made
him at thirteen an incorrigible truant; and his schoolmaster
thought it likely that he would prove a dunce. Neverthe-
less the truant schoolboy was already giving indications of
the destination of the man. At an ago too early to date
he had found iu his pen a divining rod that led him to
waters of inexhaustible delight. His mother summed up,
in the singular dialect of the district, the impression derived
from her son's boyhood and youth in the words, "he was
aye vritin." But the writing from the first, and increasingly
as time went on, could be discriminated from the ordinary
productions of boyhood. A continuity of idea, an ind»-
finable grace and freshness, marked his performances.
They were never bombastic or verbose. At no period of
his life did he suffer from a flux of words. But, boy and
man, he bad a felicitous knack of fitting words into their
right places and avoiding jerkiness and inequality. In
verse he lacked the passionate intensity required for true
rhythmic movement, but he had a fine sense of cadence
and modulation in prose
It is a curious fact that what determined Hugh Miller
to apprentice himself to a stone-mason was his delight
in literary composition. LTnemployed during the winter
frosts, the mason, ho perceived, could enjoy for some
months every year the ecstacy of writing. One result of
his decision was that he never learned any language but
English. Another was that fifteen years of the quarry and
the hewing-shed, with stern experiences of over-work and
privation, sowed in his frame the seeds of incurable disease.
Meanwhile the advantages of his decision were indisputable.
Under the discipline of labour the refractory schoolboy
became a thoughtful, sober-minded man. Miller always
looked back to his years of hand-labour with a satisfaction
tha^ has something in it of solemnity and pathos. " Noble,
upright, self-relying tod," he exclaims ; " who that knows
thy solid worth and value would be ashamed of thy hard
hands, and thy soQed vestments, and thy obscure tasks, —
thy huuible cottage, and hard couch, and homely fare !"
It cannot be added that his fifteen years of close and
constant intercourse with fellow-workmen inspired him with
much respect for their class. He was most unfortunate
in his comrades during the two seasons, 1824 and 1825,
when he worked at Niddrie in the neighbourhood of
Edinburgh. Swinish in their enjoyments, meanly selfish
in their class ambitions, and fatuously subject to talking
charlatans, that Niddrie squad of reprobates which he de-
scribes in J/y Schools and Schoobnaslers stamped on the
mind of Hugh Miller an indelible conviction of the inca-
pacity and degradation of the hand-workers.
Returning to Cromarty, he worked in happy patience „«
a stone-cutter year after year, sedulously prosecuting at
the same time the grand object of his ambition, to write
good English. He found time to invigorate and enrich his
mind by careful reading, and was habitually and keenly
observant both of man and of nature. His reading was
not extensive but well chosen, and embraced Locke and
Hume ; Goldsmith and Addison were, more than any
others, his masters in style. It was to get time to ^n■ite that
he had become a stone-mason ; another of the surprises of
his career is that it was in advertising himself as a mason
that he came before the world as a literary man, A stone-
mason, figiiring as a poetical contributor to the Inverness
Courier, might, he thought, be asked by some of the
readers to engrave inscriptions on tombs. He therefore
forwarded some of his verses to the editor. These seem
to have been consigned to the waste-paper basket, which
had been the fate of an " Ode on Greece " offered to the
Scotsman when he was at Edinbuigh. Piqued by his
second failure, he now resolved, at all hazards, to see him-
self in print. In 1829 appeared the small volume contain-
ing Poems TTritlen in the Leisure Hours of a Journei/man
-Uasoii. It procuied its author the valuable friendship of
Mr Robert Carruthers, and was favourably noticed by the
press. Miller looked at his poems in print, and concluded,
at once and irreversibly, that he woiUd not succeed as a
poet. It was a characteristic and very manly decision,
proving that there was no fretting vanity in his disposition.
Doubtless also it was right. His field was prose. But,
though his poems yielded nothing in the way of fortune,
they were a beginning of fame. The simple natives o(
Cromarty began to think him a wonder. Some very elo>
MILLER
319
qnent lettere on the herring fishery extended his reputation.
Good judges in Edinburgh detected in his work the mint-
mark of genius, and Miller's first prose volume, Scenes and
Legends of Cromarty, was published there in 1835. In the
interval he had become the accepted lover of Miss Lydia
Fraser, a young lady of great personal attractions, rare in-
tellectual gifts, and glowing sympathy with all that was
good and brave and bright. Her affection naturally
Bteadied him in hi', resolution to emerge from the hand-
working class; the mallet and chisel gradually dropped
from his grasp ; and when his prose venture appeared he
was being initiated, in Linlithgow, into the duties of a
bank clerk. ' On his return to Cromarty he found employ-
ment in the local branch of the Commercial Bank. '"_
He was a married man, and his tent seemed stably fi[xed
at Cromarty, when the agitation that preceded the Disrup-
tion of 18 is made the air of Scotland vibrate. Miller
loved his church, and deliberately esteemed her the most
valuable institution possessed by the Scottish people.
Fervently as he had sympathized with those who procured
political representation for Scotland by the Eeform Bill, he
still more fervently took part with those who claimed that
Scottish congregations should have no pastors thrust upon
them. In the summer of 1839 he wrote his famous
pamphlet-letter to Lord Brougham ; Dr Candlish read it
\rith "nothing short of rapture"; and the first days of
1840 saw Miller installed in the editorial chair of the Witness
newspaper, published twice a week in Edinburgh to advo-
cate the cause of non-intrusion and spiritual independence.
He continued to edit the Witness till his death, which took
place in the night between the 23d and 24th of December
1856. Unremitting brain work had overtaxed a system
permanently injured by the hardships of his early mason
life; reason at length gave way, and lliller died by a pistol
bhot fired by his own hand. A post-mortem examination,
attested by four medical men of the highest character,
evinced the presence of "diseased appearances" in the
biain ; and he left a few words indicating the form taken
by the insane delusion which had mastered him.
During the three years preceding the Disruption, 'cham-
pionship of the church by Miller did more, probably, than
any other single agency to win for it the suffrage of the
Scottish people. Months before the day of separation,
the name " Free Church " was prospectively assigned to
the party proposing to sever connexion with the state ;
and, whether Hugh Miller suggested the name or did not,
he- was one of the chief architects of the institution. Nor
has the sequel shown that his labour was vain.
But long ere now an enthusiasm parallel in intensity
Kfith that which he felt for his country and his church,
and to which even his old literary enthusiasm had become
subservient, had taken possession of him. From infancy
he had been a keenly interested observer of all natural
facts and objects, and during his career as apprentice ar-^
journeyman mason he had accumulated a vast store of th.
particular information belonging to the geologist. But it
•was not until later that he expressly undertook the study
pf geology. We still find him, when twenty-seven, laying
down charts of study and production without a word about
science. When, however, he had convinced himself that
his road to the stars was not by poetry, and when the
limited success of his prose tales and literary essays in the
volume on Cromarty suggested a profound misgiving as
to the adequacy of his purely literary materials to produce
an important resvdt, he bethought him of his hoard of
ecientific knowledge, and addressed himself with the con-
centrated energy of mature manhood to geological reading
and geological researches. These, in fact, were not new
t3 him, and he was much impressed by the interest excited
among scientific readers by a geological- chanter in the
Scenes a,nd Legends, /HiS chief master was Lyell, whom
he reverenced henceforward as one of the greatest of living
men. The principal scene of his own investigations was
the Cromarty district, where he ransacked every wrinkle
of the hill-side, and traced every stratum sawn through by
the watercourse, and where, on the beach at ebb, in indurated
clay of bluish tint and great tenacity, belonging to the
Old Red Sandstone formation, he discovered and dug out
nodules which, when laid open by a skilful blow of the
hammer, displayed certain organisms that had never been
seen by a human eye. He had entered upon correspondence
with Murchison and Agassiz ; and "fellows of the Geological
Society and professors of colleges" had been brought by his
descriptions " to explore the rocks of Cromarty." Along
with the patriotic and religious enthusiasm, therefore, that
burned within him when he went to champion his church
in Edinburgh, there glowed, in the depths of his heart,
not indeed a stronger but a more gentle and perhaps a
dearer enthusiasm for that science in which, he felt per-
suaded, he had something of his own to say, something to
which the world of culture would be glad to listen. So
early as September 1840 there began tp appear in the
Witness a series of articles entitled " The Old Red Sand-
stone." They attracted immediate and eager attention ;
and the* month was not at an end when, at the meeting of
the British Association, Murchison brought them under
the notice of the geological section, presided over by LyelL
Agassiz, already familiar from Miller's correspondence
lyith the organisms described, contributed information
respecting them, and proposed that one of the most
remarkable of the fossils should be called PterUhthys
Milleri. Buckland joined warmly in the encomiums of
Murchison and Agassiz, vowing that " he would give his
left hand to possess such powers of description as this
man." The articles which met with so enthusiastic a
reception from the most eminent geologists in Europe
formed the nucleus of a book soon after published, and
entitled The Old Red Sandstone. It established MiUer's
reputation not only as an original geologist but as a
practical thinker of great sagacity, and as a lucid and
fascinating writer. He had at last fairly found his hand ;
it is impossible to turn from the Scenes and Legends to the
new volume without feeling that the spirit of the author
has become more exultant, his, touch at once stronger and
more free.
During his seventeen years of residence in Edinburgh he pablished
a variety of books, all of them more or less geological, but claiming
attention not on account of their geology alone. His First Impra-
sions of England and its People, the fruit of eight weeks' wandering
arranged in the leisure hours of a hard-worked editor, will be best
appreciated when we contrast its grace and gentleneas, the classic
jnoderation of its tone, the quiet vivacity and freshness of its
observation, ;.h« sense and sentiment and justice of its criticism,
with the smartness of the ordinary newspaper correspondent, or the
vulgarity and the impudent omniscience of the conventional book
pf travels. Apart from lis masterly descriptions, partly geological
I artly scenic, and that prose poem on the ubiquity of the ocean
which, though brief, will compare not unfavourably with select
pages from Wilson or from Kuskin, its two passages on 'Westminster
Abbey and Stratford-on-Avon would alone suffice to prove that
the Cromarty stone-mason was n man of extraordinary genius.
Of his autobiographical volume, My Schools and Schoolmasfcrs, do
opinion but one has ever been expressed. It ranks among the
finest masterpieces of its kind in the English language.
As a geologist his reputation is securely based upon his aotual
discovery of important fossil organisms, one of which bears hia
name, and on his contributions, thoroughly serviceable at the time
they were made, to our knowledge of the formation in which
those organisms occur. His eye-to-eye acquaintance with nature is
attested on every page ; and, if his enthusiasm does not often rise
into spray and surge of rapture, it is a deep ground-swell per-
ceptible in all he wrote.- His powers of observation were singularly
strong and accurate, and were accompanied with the most carcf';!
reflexion and a fine rich glow of imaginative vision. His discen;-
ment of. the true position of the ventral plate of FtericMhys, whca
S20
M I L — M I L
tt^-
the best iclitliyologista unanimously insisted on its being dorsal,
affords one of tbe nicest illustrations to be found of an obser-
vational faculty whicb reasons as wells as sees.
Ho was also, in his principal geological books, TIte FooUtcps of
the Creator and Tlie TeManonij of the Kocks, a polemical defender of
tlieiani and of revelation against some whom lie regarded as their
dendly assailants. It would have been safe and pleasant for Miller
to waive all consideration of the religious question. He would thus
have escaped the dreaded sneer of the scientific expert. He would
have escaped, also, the cold suspicion of many on his own side ;
for the groat mass of mediocre religionists like nothing so well as the
"ing of difficulties and hushing up of objections. Uut
instinctively from the moral cowardice of reserve. The
advance of science has tended to compromise some of his controvelsial
positions. When he occupied the cJiairof the Itoyal Thy sical Society
of ICdiuburgh in 1S52, ne could look the most eminent repre-
sentatives of contemporary geology in the face, and claim their
assent to the possibility of drawing dehnito lines of demarcation
between the Tertiary, Secondary, and PaWozoic strata. Ho could
sneak of " the entire typo of organic being" as altering between
tlicso i»rio<l9. "All ou the one side of the gan," lie could dare to
affirm, " belongs to one fashiou, and all on the other to another
and ulioUy tiilh-rent fosliion." In the thirty intervening years
Bvery form of tlie cataclysmal scheme of geological progression has
been lUscrodited. It has become impo<isible to obtain anythiug like
o i»/is.'Hji(s of opinion among scientific men as to the placing of
those frontier lines between [xrio^l and pericKl which, however wide
may be the margins of giaJ.ition assigned to "morning" and
"evening," are iutli-ipenaablc to the maintenance of iliUer's theory
of the six-days' vision of creation. "Geographical provinces and
zones," says Professor Huxley, "may have been as distinctly
marked iu tbe Paheozoic eixx:h as at present, and those seemingly
sudden appearances of new genera and species which we ascribe
tj new creation may bo simple results of migration." Such is now
the received opinion of geologists, and we may be sure that Sliller,
who never shut his eyes to au established fact, would have accepted
it. Ho has said iu so many words that the Bible docs not teach
science.
In the long flud memorable debate on the origin of species he
strenuously engaged, maintaining, against the author of the Vestiges,
tlie doctrine of specific creation. But when he did so he could
ieel that Buckland, Sedgwick, Jlurchisou, and Lyell were ou his
side; nor is it a paradox to allege that he was an ally of Darwin
himself. If the author of the Fcs/ir^w was right, Darwin was wrong-
Ill jjoiut of fact, the former was very nearly right ; but, precisely
because Darwiu supplies what is lacking in his argument, those who
intelligently asseut to tbe Origin of SjKcics are bound not to assent
to the Vestiges.
But it is chiefly perhaps in connexion with the sweetness and
classical auiiuation of his style, and the lovely views he gives of
nature's facts, that we ought to praise Hugh ililler. In an age
prodigal of genius, yet abounding also in extravagance, glare, and
()ombast, tho self-educated stone-mason wrote with the calmness
and moderation of Addison. His powerful imagination was dis-
eiidined to draw just those lines, and to lay on just those colours,
which should reanimate tho ]iast. As his friend Carruthers, all
admirable critic of style, observed, "the fossil remains seem, iu
his glowing jviges, to live and llourisli, to fly, swim, or gambol,
or to shoot uji in vegetative profusion and splendour, as in the
iirinial dnwn of creation. Such power belongs to high genius."
Tens of tlioufauds he has incited to the study of nature ; tens of
thonsandt he has taught to find iu geology no mere catalogue of
defunct organisms, no dreary sermon in fossil stones, but a "science
of landscape" as well as au intelligent undeistandiug of the rocky
framework of the world.
In 1S71 nppenred The Life and Utiert of I7ti^h ifitler, by Peter Bayno
(2roI»., Loni
ippeo
edition of twcoty volu
circulated on the Hiiropoun continent,
Tlicy have buon Issued In the United Stalci
nprUlng tlie Life and Letters. (P. B.)
MILLER, ■William (17S1-1849), the founder of an
American religious sect holding peculiar millennarian view.s,
■was born at Pittsfield, Massachusetts, in 1781. He received
1 very imperfect education. In the war of 1812 he served
ns cajitain of volunteers on the Canadian frontier. While
residing at Low Hampton, N.Y., he began in 1833 publicly
to lecture on the subject of the millennium, asserting that
the second coming of Christ would take place in about
ten years. Hia doctrines awakened wide interest among
certain classes of the community. In 1810 a semi-monthly
journal, 7'he Signs of (he 'Times, was started by one of his
followers, and two years later the Acheiut Herald made its
.appearance. About 18-13 the second coming of Christ was
expected by as many as 50,000 believers in the doctrines of
Miller ; and, although the disappointment of their hope*
somewhat diminished their numbers, many continued their
adherence to his tenets regariiing the nature of the niillen-
niura. At present tho nunil>er of Millerites or Adventists is
estimated at from 15,000 to 20,000. Miller died at New
Hampton, Washington county, N.Y,, December 20, 1849.
JIILLER, William (170C-1882), one of the greatest
of modern line-engravers, was born in Edinburgh on the
28th of May 1796. After studying in London under
George Cook, a pupil of Easire's, he returned to his
native city, where he continued to practise his art during
a long lifetime. He executed plates after Thomson of
Duddingston, MaccuUoch, D. O. Hill, Sir George Harvey,
and other Scotti.sh landscapists, but his most admirable
and most vohtminous works were his transcripts from
Turner. The first of these was the CloveUy (1824), of The
Soiil/iem Coast, a pubUcation undertaken by his master
and his brother William B. Cook, to which Miller also con-
tributed the Combe Martin and the Portsmouth. He
was engaged on the illustrations of England and Wales,
1827-38 ; of The Bivers oj France, 1833-35 ; of Roger's
Poems, 1834 ; and very largely on those of The Prose and
Poetical Works of Sir Waller Scott, 1834. In The Pro-
vincial Antiquities and Pictvresqite Scenery of Scotland,
182G, ho executed a few excellent plates after Thomson
and Turner. Among his larger engravings of Turner's
works may be mentioned The Grand Canal, Venice ; The
Rhine, Osterprey, and Feltzen ; The Bell Rock ; The Tower
of London; and The Shepherd. The art of William Miller
was warmly appreciated by Turner himself, and Mr Ruskin
has pronounced liim to be on the whole the most successful
translator into line of the paintings of the greatest English
landscapist. His renderings of complex Turnerian sky-
effects are especially deUcate and masterly. Towards the
end of his life Miller abandoned engraving and occupied his
leisure in the production of water-colours, many of which
were exhibited in the Royal Scottish Academy, of which
he was an honorary member. He resumed his burin,
however, to produce two final series of vignettes from
dramngs by Birket Foster illustrative of Hood's Poems,
pubhshed by Moxon in 1871. Miller was a much
respected member of the Society of Friends. He died
while on a visit to Sheffield, on the 20th of January
1882.
-MILLER'S THUMB (Coltmgobio), a weU-known little
fish, abundant in all rivers and lakes of northern and
central Europe with clear water and gravelly bottom.
The genus Cottus, to which the ililler's Thumb belongs, ia
easily recognized by its broad, flat head, rounded and
scaleless body, large pectoral and narrow ventral fins, 'with
two dorsal fins, the anterior shorter than the posterior ;
the praiopercidum is armed ■n-ith a simple or branched
spine. The species of the genus Cottus are rather numerous,
and are confined to tho north temperate zone of the globe,
the majority being marine, and known by the name of "Bull-
heads." The Miller's Thumb is confined to freshwater;
and only one other freshwater species is found in Europe,
C. pa'cilopiis, from rivers of Hungary, Gahcia, and the
Pyrenees ; some others occur in the fresh waters of northern
Asia and North America. The Miller's Thumb is common
in all suitable localities in Great Britain, but is extremely
rare in Ireland ; in tho Alps it reaches to an altitude
exceeding 7000 feet. Its usual length is from 3 to 5
inches. Generally hidden under a stone or in a hollow of
the bank, it watches for its jircy, which consists of small
aquatic animals, and darts when disturbed with extra-
ordinary rapidity to some other place of refuge. Tlie
female deposits her ova in a cavity under a stone, whilst
the male watches and defends them until the young art
hatched and able to shift for themselves.
MILLET
321
MILLET (French, millet ; Italian, miglietto, diminutive
t)f m!^/to = Latin mille, a thousand, in allusion to its
fertility) is a name applied with little deSniteness to a con-
siderable number of often very variable species of cereals
belonging to distinct genera and even subfamilies of
Gramiaex. The true millet, however, is generally admitted
to be Panicum (^Setana) miliaceum, L. (German Hirce,
\»ith which P. miliare. Lam., is reckoned by some
Ixjtanists). It is indigenous to the East Indies and North
Australia, but Ls meationed by Hippocrates and Theo-
phrastus as already cultivated in South Euiope in their
time. Some suppose it to be one of the earliest grains used
in bread-making, and ascribe the origin of its name to panis,
bread, rather than to the paniculate inflorescence. It is
annual, requires rich but friable soO, grows to about 3 or 4
feet high, and is characterized by its bristly, much branched
nodding panicles. One variety has black grains. It is
largely cultivated in India, southern Europe, and northern
Africa, and ripens as far north as southern Germany, in
fact, wherever the climate admits of the production of wine.
The grain, which is very nutritious,
is used in the form of groats, and
makes excellent bread when mixed
with wheaten flour. It is aiso largely
-used for feeding poultry and cage-
birds, for which purpose mainly it is
imported. P. italicum, L. (Setaria
italica, Beauv.), is of similar origin
and distribution, and is one of the
most wholesome and palatable Indian
cereals. It i^ annual, grows 4 to 5
feet high, and requires dry light soil.
German Millet (P. germanicum, Ger-
man Kolbcnhirse, Mohar) is probably
merely a less valuable and dwarf
variety of P. italicum, having an
erect, compact, and shorter spike.
The grains of both are very small,
only one half as long as those of
common millet, but are exceedingly
prolific. Many stalks arise from a
single root, and a single spike often
yields 2 oz. of grain, the total yield
being five times that of wheat. They
are imported for poultry feeding like
the former species, but are extensively
used in soups, Ac, on the Continent.
Numerous other species belonging to
this vast genus — the largest among grasses, of which the
following are among the most important — are also culti-
vated in tropical or sub-tropical coimtries for their grain or
as fodder grasses, or both, each variety of soil, from swamp
to desert, having its characteristic forms. They are very
readily acclimatized wherever the temperature is sufficient,
e.g., in Australia, and seem destined to ri$e in agricultural
importance.
Polish Millet is P. digitaria ; P. frumenlaceum, Roxb. , Shamalo,
a Deccan grass, Is probably a native of tropical Africa ; wliile the
perennial P. sarmentosutn, Ro-xb., also largely cultivated in tropical
countries, is from Sumatra. P. daomposiltim is the Australian
millet, its grains being ;nade into cakes by the aborigines. P.
maximum, Jacq,, is the Guinea Grass ; it is perennial, grows 8 feet
high, and j-ieMs abundance of higlily nutritious grain. P. spec-
tabih, Nees. , is the Coapim of Angola, but has been acclimatized in
Brnzil and other tropical countries. Other gigantic species 6 or 7
feet higli form the field crops on the banks of the Amazons. Of species
belonging to allied genera, Peniiiseium ihyphoitUum, Rich. {Pcni-
mtlaria spicaJa, Willd.), Bnjree, sometimes also called Eg>-ptian
Millet, a Guinea corn, is largely cultivated in tropical Asia, Nubia,
.ind Egypt. P. dislichum provia sonth of the Sahara. Species of
Paspalum, EUuMne, and ililium are also cultivated as millets.
But the most important dry grain of the tropical coun trigs
of Africa and Asia, particularly of India, is Sorghum vulgare,
Pera. (IIolcus Sorghum, L., Andropogon Sorghum, Roxb.),
Durra, Great Millet, Indian Miikt, Turkish Millet, or
Guinea Corn (the French
sorgho, German Mohren-
hirse or Kaffemkom, Ta-
mil Cholum, Bengalese
Jowari). It ranges prob-
ably as extensively as <>?^Jj*-asj
wheat, being also largely "^Jf^^V .
cultivated in southern - •^.i\
Europe, tho United
States, and the West
Indies. In Asia Minor,
Arabia, Italy, and Spain
it may be said to replace
cats and barley. It is
annual, and may reach
12 feet in height; it is
extremely prolific, even
rivalling maize, of which
it is a near congener. Its
flour is very white, but
does not easily make good
bread ; it is largely used
in cakes and puddings
and for feeding cattle and
poultry. The panicles are
used for brooms, and the
roots for velvet>brushes. Tin. %— Sorghum vulgare.
S. bicolor, S. nigrum, S. ruhrum, S. Kafrorum (Kaffre
Corn), S. saccharainm, and other species or varieties are
also of economic importance, the last-named (the " Chinese
sugar-cane") being much cultivated in the United States as
a source of molasses, the juice, which contains much glucose
but comparatively little cane sugar, being simply expressed
and concentrated by evaporation. S. vulgare is the grain
referred to by Pliny as millet.
For systematic and economic purposes, see Grasses ; Luersseu,
Mcd.-Pharm. Bolanik, Leipsic, 1880; Drury, Useful Plants of
India, London, 1873 ; F. v. JliiUer, Select Plants for Naturaliza-
tion in Victoria, Melbourne, 1876. For archseology, see Hehn's
KuUurpJlanxn, kc, Berlin, 1877. On Sorghum cerunum ("rice
com," &u. , of western Kansas) see Drummond's "Report" in Pari.
Papers, No. 2570 (1880).
MILLET, Jean FEAugois (1814-1875), was a painter
of French peasant life, and it may be questioned whether
France has produced in our day any greater or more
original artist. He himself came of a peasant family, and
was born on the 4th of October 1814 in the hamlet of
Gruchy, near Gr^ville (La Manche), in the wild and
picturesque district called La Hague. His boyhood was
passed working in his father's fields, but the sight of the
engravings in an old illustrated Bible set him dra\ving, and
thenceforth, whilst the others slept, the daily hour of rest
was spent by Millet in trying to render the famiUar scenes
around him. From the village priest the lad learnt to read
the Bible and Virgil in Latin, and acquired an interest in
one or two other works of a high class which accompanied
him through life ; he did not, however, attract attention
so much by his acquirements as by the stamp of his mind.
The whole family seems, indeed, to have worn a character
of austerity and dignity, and when Milljt's father finaUy
decided to test the vocation of his son as an artist, it was
with a gravity and authority which recalls the patriarchal
households of Calvinist France. Two drawings were pre-
pared and placed before a painter at Cherbourg named
Mouchel, who at once recognized the boy's gifts, and
accepted him as a pupil; but shortly after (l835) Millet's
father died, and the eldest son, with heroic devotion, took
his i^lace at home, nor did he return to his work until the
JCVL — 41
322
M I L — M I L
pressing caUa from without were solemjily enforced by the
wishes of his own family. He accordingly went bac^k to
Cherbourg, but after a short time spent there with another
master (Langlois) started with many misgivings for Paris.
The council-general of the department had granted him a
sum of 600 francs, and the town council promised an
annua! pension of 400, but in spite of friendly help and
introductioas Millet went through great difficulties. The
system of the ficole des Beaux Arts was hateful to him,
and it was not until after much hesitation that he decided
to enter an official studio — that of Delaroche. The master
was certainly puzzled by his pupil ; he saw his ability,
and, when Millet in his porerty could not longer pay the
monthly fee's, arranged for his free admission to the studio,
but he tried in vain to make him take the approved direc-
tion, and lessons ended with " Eh, bien, allez i votre guise,
V0U3 ^tes si nouveau poiur moi que je ne veux rien vous
dire." At last, when the competition for the Grand Prix
came on, Delaroche gave Millet to understand that he
intended to secure the nomination of another, and there-
upon Millet withdrew himself, and with his friend Marolle
started in a little studio in the Eue de I'Est. He had
renounced the beaten track, but he continued to study
hard whilst he sought to procure bread by painting por-
traits at 10 or 15 francs a piece and producing small
" pastiches " of Watteau and Boucher. These works are
classed as those of his " flowery manner," and Millet has
been reproached — he whose whole Efe was an act of con-
viction— with having sacrificed his convictions to curry
favour with the public. It is true that he himself has
recorded his aversion to both these masters. "In the
Lpuvre," he said, "I received vivid impressions from
Mantegna, complete from Michelangelo ; after Michelangelo
and Poussin I have remained faithful to the early masters."
Boucher was for him an object of "repulsion," and in
Watteau "I saw," he said, "a little theatrical world which
oppressed me." Thus it was then that Millet naturally
felt and saw, but the strongest genius knows moments of
self-doubt. Later in life Millet was heard to say that
were it not for the small group who beli»ved in him he
should have lost faith in himself. In earlier years, before
he was certain of his own leading, he was naturally influ-
enced by the advice of others whose arguments were enforced
by the pressure of dire poverty. Even so from time to
time the native vein showed strong. In 1840, as soon as
he had despatched a portrait tcf the Salon, MUlet went back
to Gr^ville, where he painted Sailors Mending a Sail and a
few other pictures — reminiscences of Cherboui'g life. His
first success was obtained in 1844 when his Milkwoman
and Lesson in Riding (pastel) attracted notice at the Salon,
and friendly artists presented themselves at his lodgings
only to learn that his wife had just died, and that he him-
self had disappeared. Millet was at Cherbourg ; there he
remarried, but having amassed a few hundred francs he
went back to Paris and presented his St Jerome at the
Salon of 1845. This picture was rejected and exists no
longer, for Millet, short of canvas, painted over it Qidipus
Unbound, a work which during the following year was the
object of violent criticism. He was, however, no longer
alone ; Diaz, Eugene Tournoux, Rousseau, and other men
of note supported him by their confidence and friendship,
and he had by his side the brave Catharine Lemaire, his
second wife, a woman who bore poverty with dignity and
gave courage to her husband through the cruel trials in
which he penetrated by a terrible personal experience the
bitter secrets of the very poor. To this date belong
Millet's Golden Age, Bird Nesters, Young Girl and Lamb,
and Bathers; but to the Bathers (Louvre) succeeded The
Mother Asking Alms, The Workman's Monday, and The
Winnower. This last work, sxhibited in 1848, obtained
conspicuous success, but did not sell till Ledru Rollin,
informed of the painter's dii-e distress, gave him 500 franca
for it, and accompanied the purchase with a commission,
the money for which gnabled Millet to leave Paris for
Barbizon, a village on the skirts of the forest of Fontaine-
bleau. There he settled in a three-roomed cottage for tho
rest of his life — twenty-seven years, in which he wrought
out the perfect story of that peasant life of which he alone
has given a " complete impression." Jules Breton has
coloured the days of toil with sentiment ; others, like
Courbet, whose eccentric Funeral at Ornans attracted more
notice at the Salon of 1850 than Millet's Sowers and
Binders, have treated similar subjects as a vehicle for
protest against social misery ; Millet alone, a peasant and
a miserable one himself, saw true, neither softening nor
exaggerating what he saw. In a curious letter written to
M. Sensier at this date (1850) Millet expressed his resolve
to break once and for all with mythological and uudraped
subjects, and the names of the principal works painted
subsequently will show how stedfastly this resolution was
kept. In 1852 he produced Girls Sewing, JIan Spreading
Manure; 1853, The Reapers; 1854, Church at "Gr^ville
(Luxembourg) ; 1855 — the year of the international
Exhibition, at which he received a medal of second class —
Peasant Grafting a Tree ; 1857, The Gleaners ; 1859, The
Angelas (Louvre, engraved Waltner), The Woodcutter and
Death; 1860, Sheep Shearing; 1861, Woman Shearing
Sheep, Woman Feeding Child; 1862, Potato Planters,
Winter and the Crows; 1863, Man with Hoe, Woman
Carding; 1864, Shepherds and Flock, Peasants Bringing
Home a Calf Born in the Fields ; 1869, Knitting Lesson :
1870, Buttermaking ; 1871, November — recollection of
Gruchy. Any one of these works vrill show how great an
influence Millet's previous practice in the nude had upor.
his style. The dresses worn by his figures are not clothes,
but drapery through which the forms and movements of the
body are strongly felt, and their contour shows a grand
breadth of line which strikes the eye at once. Something
of the imposing unity of his work was also, no doubt, due
to an extraordinary power of memory, which enabled
Millet to paint (like Horace Vernet) without a model ; he
could recall with precision the smallest details of attitudes
or gestures whioli he proposed to represent. Thus he could
count on pre^mting free from after thoughts tho vivid
impre-'sions whiil.he had first received, and Millet's nature
was such that the impressions which he received were
always of a serious and often of a noble order, to which
the character of his execution responded so perfectly thit
even a Washerwoman at her Tub will show the grand
action of a Medea. The drawing of this subject. is repro-
duced in Souvenirs de Barbizon, a pamphlet in which M.
Piedagnel has recorded a visit paid to Jlillet in 1864.
His circumstances were then less evU, after struggles as
severe as those endured in Paris. A contract by which
he bound himself in 1860 to give up all his work for
three years had placed him in possession of 1000 francs
a month. His fame extended, and at the exhibition of
1867 he received a medal of the first class, and the
ribbon of the Legion of Honour, but ho was at the same
moment deeply shaken by the death of his faithful friend
Rousseau. Though he rallied for a time he never com-
pletely recovered his health, and on the 20th January
1876 he died. Ho was- buried by his friend's side in the
churchyard of Chailly.
See A. Sensier, Tic et (Euvrt dt J. F. ifillei, 1874 ; PiMagnel,
Souvenirs dc Barbizon, &c. (E. F. S. P.)
MILLVILLE, a city of the United States, in Cumberland
county. New Jersey, at tho head of navigation of Maurice
river, 40 miles by rail from Philadelphia by the Capo May,
Millville, and Vineknd section of the West Jersey Railroad.
M I L — M I L
323
It is one of the chief seats of glass-making in the State,
and also manufactures cotton, iron pipes for water and gas,
turbines, itc. The population was 7660 in 1880.
JUXMAN, Henky Ham (1791-1868), dean of St
Paul's, was bom February 10, 1791, and was the third
son of Sir Francis Milman, physician to George IIL He
was educated at Eton and at Brasenose College, Oxford ;
his university career was brilliant, and among other dis-
tinctions he gained the Newdigate prize with a poem on
the Apollo Belvedere. In 1816 he was ordained, and was
soon afterwards presented to the living of St Mary's,
Reading. He had already made his appearance as a
dramatic writer, his tragedy of Fazio, founded on a narra-
tive in the Annual Eeguteriov 1795, having been brought
on the stage without his knowledge under the title of The
Italian Wi/e. It was subsequently produced at Covent
Garden, and obtained great success from the acting of
Miss O'Neill as Bianca. The merit of the play consists
chiefly in the powerful situation ; the diction is florid and
ornate. The same criticism, by the author's own confes-
sion, applies to his epic, Samor, the Lord of the Bright
City (Gloucester), a poem written in early youth. 'The
subject is taken from British legend, and Milnian has failed
to invest it with serious interest. He was more successful
in his ne.xt attempts, where the subjects were well adapted
to an imagination easily kindled by the historical or the
moral picturesque. The death struggle of an expiring
nation in the Fall of Jerusalem (1820), the conflict of new
truth and old order, of religious enthusiasm and earthly
affection, in the Martyr of Antioch (1822), are depicted
\vith great eloquence and real insight into human nature.
Milman's characters, however, are personified tendencies
rather than personages, and in poetical style he was unable
to free himself from the influence of Byron. Belshazzar
(1822) is in general a pale copy of Byron's Sardanapalus,
but contains some fine lyrics. Milman's lyrics, indeed,
especially his hymns, have frequently a fine ring and sweep,
though the thought is generally commonplace. His
tragedy of Anne Boteyn (1826) is a poor performance.
With the exception of admirable versions of the Sanskrit
episode of Nala and Damayanti, and of the Agamemnon
end Bacchse, this was Milman's last poetical work. He
was elected professor of poetry at Oxford, and in 1827
delivered the Banipton lectures, selecting as his subject the
conduct and character of the apostles as an evidence of
Christianity. In 1830 his History of the Jews appeared in
the Family Library. The contracted limits of this series
forbade any adequate treatment of the subject ; the work
is nevertheless memorable as the first by an English
clergj-man which treated the Jews as an Oriental tribe,
recognized sheikhs and emirs in the Old Testament, sifted
and classified documentary evidence, and evaded or
minimized the miraculous. Slilman was violently attacked,
especially by Dr Faussett and Bishop Mant, and the odium
thus occasioned stopped the publication of the Family
Library, and long impeded the preferment of the writer.
In 1835, however, Sir Robert Peel made him rector of St
Margaret's and canon of Westminster, and in 1849 he
became dean of St Paul's. The unpopularity attaching to
him had by this time nearly died away ; and now, generally
revered and beloved, intimate with men of ajl pursuits,
politics, and persuasions, counted among the chief ornaments
of the most pohshed society of the metropolis, he occupied
a singularly dignified and enviable position, which he
constantly employed for the promotion of culture and
enlightenment, and in particular for the relaxation of
subscription to ecclesiastical formularies. His History of
Christianity under the Empire had appeared in 1840, but
had been as completely ignored as if, said Lord Melbourne,
the clergy had taken a universal oath never to mention it
to any one. Widely different was the reception of the
continuation, his great History of Latin Christianity to
the death of Pope Nicholas V.'. which appeared in 1860.
He also edited Gibbon and Horace, and at his death in
1868 left behind him almost finished a delightful history
of his own cathedral, which was completed and published
by his son.
Miln^an possessed a large share of the imagination which enters
into and calls up the past, and of that which interprets actions and
apprehends opinions by the power of sympathy. In creative
imagination he was deficient, a defect which alone prevented him
from attaining the first rank as an historian. Hia pages arc
crowded with splendid names rather than with living personages ;
the springs of action are disclosed with rcntarkable penetration, but
the actor himself is rather heard than seen. There are, however,
exceptions, such as his portrait of Sir Christopher Wren ; and
he possessed a peculiar power of investing mere intellectual
tendencies with personality and life. Jlis parallel of Latin and
Teutonic Christianity, for example, is a piece of finished historical
character painting. His power of sympathy rendered him in elTect,
as his natural equity and benignity made him in intention, a
model of historical candour, only cliargeable, perhaps, with too much
gentleness. It will be long ere his great woik is superseded ; but he
will perhaps be remembered even longer as an embodiment of all
the qualities which the higher ecclesiastical preferment can be
supposed capable of-cncouraging or rewarding among the clergy.of
a great historical church. (R. G.)
MILO, one of the most famous athletes of Greece,
whose name became proverbial for personal strength.
He lived about the end of the 6th century B.C., was six
times crowned at the Olympic games and six times at the
Pythian for wrestling, and was famous throughout the
civilized world for his feats of strength, such as carrying
an ox on his shoulders through the stadium at Olympia.
In his native city of Crotona he was much honoured, and
he commanded the army which defeated the people of
Sybaris in 511 B.C. When Democedes, the physician of
Darius, deserted the Persian service, he sent a boastful
message to the king of Persia informing him of his
marriage to the daughter of Milo. The traditional account
of his death is often used to point a moral : he found a
tree which some woodcutters had partially split with a
wedge, and attempted to rend it asunder; but the wedge
fell out, and the tree closed on his hand, imprisoning him
till wolves came and devoured him.
MILO was the surname of T. Annius Papianus, one of
the best-known of the partisan leaders and ruffians in the
stormy times that preceded the dissolution of the Roman
republic. His father was C. Papius Celsus, but he was
adopted by his mother's father T. Annius Luscus. He
joined the Pompeian party, and led the band of mercenaries
and gladiators which was required to defend the cause and
its chief supporters in the public streets. P. Clodius, the
leader of the ruflians who professed the democratic cause,
was his personal enemy, and their brawls in the streets and
their mutual accusations in the law courts lasted for several
years, beginning when Jlilo was tribune of the commons
in 57 B.C. In 53 their quarreb came to a height when
Milo was candidate for the consulship and Clodius for the
prajtorship ; and when the two leaders met by accident on
the Appiau Way at Bovill^, Clodius was murdered (January
20, 52 B.C.). This act of violence strengthened the hands
of Pompey, who was nominated sole consul, and proposed
several stringent laws to restore order in the city. Milo
was impeached; his guilt was clear, and his enemies took
every means of intimidating his supporters and his judges.
Cicero was afraid to deliver the speech he had prepared
Pro Milone, and the extant oration is an expanded form of
the unspoken defence. Milo went into exile at ilassilia,
and his property was sold by auction. He joined the
insurrection of M. Coelius in 48 B.C., and was soon slain
near Thurii in Lucania. His wife Fausta was daughter
of the dictator Sulla.
MILTLADES. See Greece, vo!. xi. p. 99.
324
MILTON
MILTON, John (1G08-1674), was born in Bread Street,
Clicapsidp, London, on the 9th of December 1008. His
father, known as Mr John Milton of Bread Street, Bcrivener,
was himself an interesting man. He was a ' native of
Oifordstire, having been born there in or about 1563, the
fior; of a Richard Milton, yeoman of Stanton-St^John's,
of 'Phom there are traces as one of the sturdiest adherents
to the old Roman Catholic religion that had been left in his
district. The son, however, had turned Protestant, ,jind,
having been cast oS on that account, had come to London,
apparently about the year 1586, to push his fortune.
Having received a good education, and having good abilities,
especially in music, he may have lived for some time by
musical teaching and practice. Not till 1595, at all event.*,
when he was long past the usual age of apprenticeship, do
we hear of his preparation for the profession of a scrivener;
and not till February 1599-1600, when he was about thirty-
seven years of age, did he enter the profession as a qualified
member of the Scriveners' Company. It was then that he
set up his " house and shop " in Bread Street, and began,
like other scriveners, his lawj'erly business of drawing up
ivills, marriage-settlements, and the like, with such related
business as that of receiving money from clients for invest-
ment and lending it out to the best advantage. It was at
the same time that he married. Till recently there has
been the most extraordinary uncertainty as to the maiden
name of his wife, the mother of the poet. It has been
now ascertained, however, that she was a Sarah Jeffrey,
one of the two orphan daughters of a Paul Jeffrey, of St
Swithln's, London, " citizen and merchant-taylor," originally
from Essex, who had died before, 1583. At the date of
her marriage she was about twenty-eight years of age.
Her widowed mother, Mrs EUen Jeflrey, came to reside in
the house in Bread Street, and died there in February
1610-11. Before this death of the maternal grandmother,
three children had been born to the scrivener and his vrife,
of whom only two survived, — the future poet, and an elder
sister, called Anne. Of three more children, born subse-
quently, only one survived, — Christopher, the youngest of
the family, born December 3, 1615.
The first sixteen years of Milton's life, coinciding exactly
with the last sixteen of the reign of James I., associate
themselves with the house in Bread Street, and with the
surroundings of that house in Old London. His father,
v.'hile prospering in business, continued to be known as a
man of " ingenioso " tastes, and even acquired some dis-
tinction in the London musical world of that time by his
occasional contributions to important musical publications.
Music was thus a part of the poet's domestic education
from his infancy, \\1iatever else could be added was
added without stint. Again and again Milton speaks with
gratitude and affection of the ungrudging pains bestowed
by his father on his early education. " Both at the
grammar school and also under other masters at home," is
the statement in one passage, " he caused me to be
instructed daily." This brings us to about the year 1619,
■when Milton was ten years of age. At that time his
domestic tutor was Thomas Young, a Scotsman from Perth-
shire, and graduate of the university of St Andrews, after-
wards a man of no small distinction among the English
Puritan clergy, but then only curate or assistant to some
parish clergyman in or near London, and eking out his
livelihood by private teaching. Young's tutorship lasted
till 1622, when ho was drawn abroad by an offer of the
pastorship or chaplaincy to the congregation of English
merchants in Hamburg. Already, however, for a year or
two, his tutorship had been only sujiplcmentary to the
education which the boy was receiving by daily attendance
at St Paul's public school, close to Bread Street. The
ieadmaster of the school was Jlr Alexander Gill, an elderly
Oxford divine, of high reputation for scholarfcip and
teaching ability. Under him, as usher or second master,
was his .son, Alexander Gill the younger, also an Oxford
graduate of scholarly reputation, but of blistering character.
Milton's acquaintance.ship with tliis younger Gill, begun at
St Paul's school, led to subsequent friendship and corre-
spondence. Far more affectionate and intimate was the
friendship formed by Milton at St Paul's with a certain
young Charles Diodati, his schoolfellow there, the son of a
naturalized Italian physician, Dr Theodore Diodati, who
had settled in London in good medical practice, and was
much respected, both on his own account, and as being the
brother of the famous Protestant divine, Jean or Giovanni
Diodati of Geneva. Young Diodati, who was destined for
his father's profession, left the school for Oxford Universit}'
early in 1623; but Milton remained till the end of 1624.
A family incident of that year was the marriage of his
elder sister, Anne, with Edward Phillips, a clerk in the
Government office caUed the Crown Office in Chancery.
Milton had then all but completed his sixteenth year, and
was as scholarly, as accomplished, and as liandsome a
youth as St Paul's school had sent forth. We learn from
himself that his exercises "in English or other tongue,
prosing or versing, but chiefly this latter," had begun to
attract attention even in his boyhood. Tin's implies that
he must have had a stock of attempts in English and Latin
by him of earlier date than 162-1. Of these the only
specimens that now remain are his Paraphrase on Psalm
CXir. and his Paraphrase on Psalm CXXXVI.
On February 12, 1624-25, Milton, at the age of sixteen
years and two months, was entered as a student of Christ's
College, Cambridge, in the grade of a " Lesser Pensioner."
His matriculation entry in the books of the university is
two months later, April 9, 1625. Between these two dates
James I. had died, and had been succeeded by Charles L
Cambridge University was then in the full flush of its
prosperity on that old system of university education
which combined Latin and Greek studies with plentiful
drill and disputation in the scholastic logic and philosophy,
but with little of phj'sical science, and next to no mathe-
matics. There were sixteen colleges in all, dividing among
them a total of about 2900 members of the university.
Christ's College, to which Milion belonged, ranked about
third in the university in respect of numbers, counting
about 265 members on its books. The master was Dr
Thomas Bainbrigge ; and among the thirteen fellows were
Mr Joseph Meade, still remembered as a commentator on
the Apocalypse, and Mr William Chajjpell, afterwards an
Irish bishop. It was under Chappell's tutorship that
Milton was pl'.ced when he first entered the college. At
least three students who entered Christ's after Jlilton, but
during his residence, deserve mention. One was Edward
King, a youth of Irish birth and high Irish connexions,
who entered in 1626, at the ago of fourteen ; another was
John Cleveland, afterwards known as royalist and satirist,
who entered in 1627; and the third was Henry More, sub-
sequently famous as the Cambridge Platonist, who entered
in 1631, just before Milton left. Milton's own brother,
Christopher, joined him in the college in February 1630-
31, at the age of fifteen.
Milton's academic course lasted seven years and five
months, or from February 1624-25 to July 1632, bringing
him from his seventeenth year to his twentyfourtL Tho
first four years were his time of undcrgraduateship. It
was in the second of these, tho year 1G26, that there
occurred that quarrel between him and his tutor, Mr
Cliappell, which Dr Johnson, making tho most of a lax
tradition from Aubrey, magnified into tho supposition that
Milton may have been one of the la>t students in cither of
the English universities that suffered tho indignity of
MILTON
32ff
corporal punishment. The legend deserves no credit ; but
it is certain that Milton, on account of some disagreemen*:
with Chappeli, leading to the interference of Dr Bainbriggo,
left college for a time, and that, when he did return, it was
under an arrangement which, while securing that he should
not lose a term by his absence, transferred him from the
tutorship of Chappeli to that of Mr Nathaniel Tovey,
another of the fellows of Christ's. From a reference to
the matter in the first of the Latin elegies one infers that
the cause of the quarrel was some outbreak of self-assertion
on Milton's part. We learn indeed, from words of his own
elsewhere, that it was not only Chappeli and Bainbrigge
that he had offended by his independent demeanour, but
that, for the first two or three years of his undergraduate-
.iliip, he was generally unpopular, for the same reason,
among the younger men of his college. They had nick-
named him " The Lady," a nickname which the students
of the other colleges took up, converting it into " The Lady
of Christ's College " ; and, though the allusion was chiefly
to the peculiar grace of his personal appearance, it con-
veyed also a sneer at what the rougher men thought his
unusual prudishness, the haughty fastidiousness of his
tastes and morals. 'Quite as distinct as the information
that he was for a while unpopular with the majority of his
fellow-students are the proofs that they all came round him
at last with respect and deference. The change had cer-
tainly occurred before January 1628-29, when, at the age of
twenty, he took his B.A. degree. By that time his intel-
lectual pre-eminence in his college,-and indeed among his
coevals in the whole university, had come to be acknow-
ledged His reputation for scholarship and literary genius,
extraordinary even then, was more than confirmed during
the remaining three years and a half of his residence in
Cambridge. A fellowship in Christ's which fell vacant
in 1630 would undoubtedly have been his had the election
to such posts depended then absolutely on merit. As it
was, the fellowship was conferred, by royal favour and
mandate, or> Edward King, his junior in coUege standing
by sixteen months. In July 1632 Milton completed his
career at the university by taking his M.A. degree. His
signature in the University Register stands at the head of
the list of those who graduated as masters that year from
Christ's. Anthony Wood's summary of the facts of his
university career as a whole is that he "performed the
collegiate and academical exercises to the admiration of all,
and was esteemed to be a virtuous and sober person, yet
not to be ignorant of his own parts." The statement is
in perfect accordance with Milton's own account. He
speaks of " a certain niceness of nature, an honest haughti-
ness, and self-esteem of what I was or what I might be,"
as one of his earliest characteristics ; and, though intimat-
ing that, even while actually a student at Cambridge, he
had " never greatly admired " the system of the place, he
leaves us in no doubt as to the quite exceptional applause
with which he had gone through all the prescribed work.
To the regular Latin and Greek of the university he had
added, he tells us, French, Italian, and Hebrew. He had
diso learnt fencing and other gentlemanly exercises of the
time, and was an expert swordsman.
Of Milton's skill at Cambridge in what Wood calls " the
collegiate and academical exercises " specimens remain in
his Prolusicmes Qusedam OralorUe. They consist of seven
rhetorical Latin essays, generally in a whimsical vein,
delivered by him, in his undergraduateship or during his
subsequent bachelorship in arts, either in the hall of
Christ's College or in the pubUc University School.
Jlelics of Milton's Cambridge period are also four of his
L?.tin Familiar Epistles; but more important are the
poetical remains. These include the greater number of his
preserved Latin poems — to wit, (1) the seven cieces which
compose his Elcgiarum Lioer, two of the most interesting
of them addre.ssed to his medical friend, Charles Diodati,
and one to his former tutor Young in his exile at Ham-
burg, (2) the five short Gunpowder Plot epigrams, now
appended to the Elegies, and (3) the first five pieces of the
S^lvartim Liber, the most important of which are the hexa-
meter poem " In Quintum Kovembris " and the piece
entitled "Naturam non pati senium." Of the English
poems of the Cambridge period the following is a dated
list -.—On the Death of a Fair Infant, 1625-2G, the subject
being the death in that inclement winter of his infant
niece, the first-bom child of his sister Mrs Phillips; At
a Vacation Exercise in the College, 1628 ; the magnificent
Christmas ode On the Morning of Christ's Nativity, 1629 ;:
the fragment called The Passion and the Song on May
Morning, both probably belonging to 1630; the lines Oil-
Shakespeare, certainly belonging to that year; the two-
facetious pieces On the University Carrier, 1630-31 ; the
Epitaph on the Marchioness of Winchester, 1631 ; the
sonnet To the Nightingale, probably of the same year ; the
sonnet On arriving at the Age of twenty-three, dating itself
certainly in December 1631
Just before Milton quitted Cambridge, his father, then
verging on his seventieth year, had practically retired
from his Bread Street business, leaving the active manage-
ment of it to a partner, named Thomas Bower, a former
apprentice of his, and had gone to spend his declining
years at Horton in Buckinghamshire, a small village near
Colnbrook, and not far from Windsor. Here, accordingly,
in a house close to Horton church, Milton mainly resided
for the next six years, — from July 1632 to April 1638.
Although, when he had gone to Cambridge, it had been
with the intention of becoming a clergyman, that intention
had been abandoned. His reasons were that "tyranny
had invaded the church," and that, finding he could not
honestly subscribe the oaths and obhgations required, he
"thought it better to preserve a blameless silence .before
the sacred oiEce of speaking begun with servitude and
forswearing." In other words, he was disgusted vdth the
system of high prelacy which Laud, who had been bishop
of London and minister paramount in ecclesiastical matters
since 1628, was estabUshing and maintaining in the Church
of England. " Church-outed by the prelates," as he
emphatically expresses it, he seems to have thought for a
time of the law. From that too he recoiled ; and, leav-
ing the legal profession for his brother Christopher, he had
decided that the only hfe possible for himself was one of
leisurely independeu'-e, dedicated wholly to scholarship and
hterature. His compunctions on this subject, expressed
already in his sonnet on arriving at his twenty-third year,
are expressed more at length in an English letter sent by
him, shortly after the date of that sonnet, and with a copy
of the sonnet included, to some friend who had been
remonstrating with him on his " belatedness " and his
persistence in a life of mere dream and study. There
were gentle remonstrances also from his excellent father.
Between such a father and such a son, however, the con-
clusion was easy. WTiat it was may be learnt from Milton's
fine Latin poem Ad Patrem. There, in the midst of an
enthusiastic recitation of all that his father had done for
him hitherto, it is intimated that the agreement between
them on their one little matter of difference was already
complete, and that, as the son was bent on a prrvate Ufe of
hterature and poetry, it had been decided that he should
have his own way, and should in fact, so long as he chose,
be the master of his father's means and the chief person in
the Horton household, j^or the six years from 1632 this,
accordingly, was Milton's position. In perfect leisure, and
in a pleasant rural retirement, with Windsor at the distance^
of an easy walk, and London only about 17 miles- 'ofi. h»
326
MILTON
-went through, he tells us, a systematic course of reading
in the Greek and Latin classics, varied by mathematics,
music, and the kind of physical science we should now call
cosmography.
It is an interesting fact that Milton's very first public
appearance in the world of English authorship was in so
honourable a place as the second foUo edition of Shakespeare
in 1632. His enthusiastic eulogy on Shakespeare, written
in 1630, was one of three anonjTnous pieces prefixed to
that second folio, along with reprints of the commendatory
verses that had appeared in the first folio, one of them
Ben Jonson's immortal tribute to Shakespeare's memory.
Among the poems actually written by Milton at Horton
the first, in all probability, after the Latin hexameters Ad
Patrem, were the exquisite companion pieces L' Allegro
and II Penseroso. There followed, in or about 1633, the
fragment called A rcades. It was part of a pastoral masque
got up by the young people of the noble family of Egerton
in honour of their venerable relative the countess-dowager
of Derby, and performed before that lady at her mansion of
Harefield, near Uxbridge, about 10 miles from Horton.
That Milton contributed the words for the entertainment
was, almost certainly, owing to his friendship mth Henry
Lawes, one of the chief court musicians of that time, whose
known connexion with the Egerton family points hmi out
as the probable manager of the Harefield masque. Next
in order among the compositions at Horton may be
mentioned, the three short pieces, At a Solemn Minic, On
I'ime, and U]>on the Circumcision ; after which comes
Comns, the largest and most important of all Milton's
minor poems. The name by which that beautiful drama
i.s now universally kno-ivn was not given to it by Milton
himself. He entitled it, more simply and vaguely, " A
Jvlasque presented at Ludlow Castle, 163-1, before the Earl
■of Bridgewater, Lord President of Wales." The existence
of this poem is certainly due to ililton's intimacy with
Lawes. The earl of Bridgewater, the head of the Egerton
family, had been appointed to the high office of the
presidency or viceroyalty of Wales, the official seat of
which was Ludlow in Shropshire ; it had been determined
that among the festivities on his assumption of the office
ttiere should be a great masque in the hall of Ludlow
Castle, with Lawes for the stage manager and one of the
actors ; Milton had been applied to by Lawes for the
poetry; and, actually, on Michaelmas night, September 29,
1631, the drama furnished by Milton was performed in
Ludlow Castle before a great assemblage of the nobility
and gentry of the Welsh principality, Lawes taking the part
»f " the attendant spirit," while the parts of " first brother,"
" second brother," and " the lady " were taken by the earl's
three youngest children, Viscount Brackley, Mr Thomas
Egerton, and Lady Alice Egerton. — From September 1634
to the beginning of 1637 is a comparative blardc in our
records. Straggling incidents in this blank are a Latin
letter of date December -1, 1634, to Alexander Gill the
younger, a Greeh Translation of Psalm CXIY., a visit to
Oxford in 1635 for the purpose of incorporation in the
degree of M.A. in that university, and the beginning in
^lay 1636 of a troublesome lawsuit against his now aged
and infirm father. — The lawsuit, which was instituted by
i\ certain Sir Thomas Cotton, baronet, nephew and executor
of a deceased John Cotton, Esq., accused the elder Milton
and his partner Bower, or both, of having, in their capacity
i\3 scriveners, misappropriated divers large sums of money
that had been entrusted to them by the deceased Cotton to
1)0 let out at interest. The lawsuit was still in progress
when, on the 3d of April 1637, Milton's mother died, at
the ago of about sixty-five. A flat blue stone, with a brief
inscription, visible on the cliancel-pavement of Horton
'ckm-ch. still inurk.^ the "kce of her burial, MiltQu's
testimony to her character is that she was a "a most
excellent mother and particularly known for her cluu'itiea
through the ueighboiu-hood." The year 1637 was other-
wise eventful in his biography. It was in that year that
his Comus, after lying in manuscript for more than two
years, was published by itself, in the form of a small quarto
of thirty-five pages. The author's name was withheld, and
the entire responsibility of the publication was assumed by
Henry Lawes. Milton seems to have been in London when
the little volume appeared. He was a good deal in London,
at all events, during the summer and autumn months
immediately following his mother's death. The plague,
which had been on one of its periodical visits of ravage
through England since early in the preceding year, was
then especially severe in the Horton neighbourhood, while
London was comparatively free. It was probably in
London that Jlilton heard of the death of young Edward
King of Christ's College, whom he had left as one of the
most popular of the fellows of the college, and one of the
clerical hopes of the university. King had sailed from
Chester for a vacation visit to his relatives in Ireland,
when, on the 10th of August, the ship, in perfectly calm
water, struck on a rock and went dowm, he and nearly
all the other passengers going down with her. There ia
no mention of the sad accident in two otherwise very in-
teresting Latin Familiar Epistles of Milton, of September
1637, both addressed to his medical friend Charles Diodati,
and both dated from London ; but how deeply the death of
King had affected him appears from his occupation shortly
afterwards. In November 1637, and probably at Horton,
whence the plague had by that time vanished, he WTOte
his matchless pastoral monody of Lycidas. It was his con-
tribution to a collection of obituary verses, Greek, Latin, and
English, which King's numerous friends, at Cambridge and
elsewhere, were getting up in lamentation for his sad fate.
The collection did not appear till early in 1638, when it
was published in two parts, with black-bordered title-pages,
from the Cambridge University press, one consisting of
twenty-three Latin and Greek pieces, the other of thirteen
English pieces, the last of which was Milton's monody,
signed only with his initials "J. M." It was therefore
early in 1638, when Milton was in his thirtieth year, that
copies of his Lycidas may have been in circulation among
those who had already become acquainted with his Comvs.
Milton was then on the wing for a foreign tour. He
had long set his heart on a visit to Italy, and circum-
stances now favoured his wish. The vexatious Cotton
lawsuit, after hanging on for nearly two years, was at an
end, as far as the elder Milton was concerned, with the
most absolute and honourable vindication of his oharacter
for probity, though with some continuation of the case
against his partner, 'Bower. Moreover, Milton's younger
brother, Christopher, though but twenty-two years of age,
and just about to be called to the bar of the Inner Temple, .
had married a wife ; and the young couple had gone to
reside at Horton to keep the old man company. There
being nothing then to detain Milton, all was arranged
for his journey. Before the end of April 1638 he
was on his way across the Channel, talcing oue English
man-servant with him. At the time of his departure
the last great news in England was that of tlie National
Scottish Covenant, or solemn oath and band of all janks
and clas.scs of the Scottish people to stand by each other
to the death in resisting the ecclesiastical innovations
which Laud and Charles had been forcing upon Scotland.
To Charles the news of this "damnable Covenant," as he
called it, was enraging beyond measure ; but to tlio maf.'i
of the English Puritans it was far from unwelcome,
promising, as it seemed to do. for England herself, the
subversion at last of that system of " Thorough," or dcspotit
\
MILTON
327
gOTemment by the king and hia ministers without parlia-
ments, under which the country had been groaning since the
contemptuous dissolution of Charles's third parliament ten
years before.
Through Paris, where Milton made but a short stay,
receiving polite attention from the English ambassador,
Lord Scudamore, and having the honour of an introduction
to the famous Hugo Girotiua, then ambassador for Sweden
at the French court, he moved on rapidly to Italy,, by way
of Nice. After visiting Genoa, Leghorn, and Pisa, he
arrived at Florence, August 1638. Enchanted by the city
and its society, he remained there two months, frequenting
the chief academies or literary clubs, and even taking- part
in their proceedings. Among the Florentines with whom
he became intimate were Jacopo (Jaddi, young Carlo Dati,
PietrO Frescobaldi, Agostino Coltellini, the grammarian
Benedetto Buommattei, Valerio Chimentelli, and Antonio
Francim. It was in the neighbourhood of Florence also
that he " found and visited " the great Qalileo, then old
and blind, and stUl nominally a prisoner to the Inquisition
for his astronomical heresy. From Florence, by Siena,
Milton went to Rome. He reached the Eternal City some
time in October, and spent about another two months
there, not only going about among the ruins and antiquities
and visiting the galleries, but mixing also, as he had done
in Florence, with the learned society of the academies.
Among those with whom he formed acquaintance in Borne
■were the German scholar, Lucas Hobtenius, librarian of
the Vatican, and three native Italian scholars, named
Cherubini, SaliQli, and Selvaggi. There is record of his
having dined once, in company with several other English-
men, at the hospitable table of the English Jesuit College.
The most picturesque incident, however, of his stay in
Bome was his presence at a great musical entertainment
in the palace of Cardinal Francesco Barberim. Here he
had not only the honour of a specially kind reception by
the cardinal himself, but also, it wpuld appear, the
supreme pleasure of listening to the marvellous Leonora
Barbni, the most renowned singer of her age. Late in
November he left Rome for Naples. Here also he was
fortunate. The great man of the place was "uie now very
aged Giovanni Battista Manso, marquis of VUla, the friend
and biographer of the great Tasso, and subsequently the
friend and patron of the sweet Marini. By a happy
accident Milton obtained an introduction to Manso, and
nothing could exceed the courtesy of the attentions paid
by the aged marquis to the young English stranger. He
had hardly been in Naples a month, however, when there
came news from England which not oixly stopped an
intention he had formed of extending his tour to Sicily
and thence into Greece, but urged his immediate return
home. " The sad news of civil war in England," he says,
" called me back ; for I considered it base that, while my
fellow-countrymen were fighting at home for liberty, I
should be travelling abroad for intellectual culture." In
December 1638, therefore, he set his face northwards again.
His return journey, however, probably because he learnt
that the news he' had first received was exaggerated or
premature; was broken into stages. He spent a second
two months in Rome, ascertained to have been January
and February 1638-39 ; during which two months, as he
tells us, he was in some danger from the papal police,
because the English Jesuits in Rome had taken offence at
hia habit of free speech, wherever he went, on the subject
of religion. Though he did not alter his demeanour in the
least in this particular, nothing happened ; and from Rome
,Jie got safely to Florence, welcomed back heartily by his
Tlorentine friends, and renewing his meetings with them
privately and in their academies. Hia second visit to
Florence, including an ezcursio" to Lucca, extended over
two months; and not till April 1639 did he take his
leave, and proceed, by Bologna and Ferrara, to Venice.
About a month was given to Venice ; and thence, having
shipped for England the books he had collected in Italy,
he went on, by Verona and MUan, over the Alps, to
Geneva. In this Protestant city he spent a week or two
in June, forming interesting acquaintanceships there too,
and having daily conversations with the great Protestant
theologian Dr Jean Diodati, the uncle of his friend
Charles Diodati. From Geneva he returned to Paris, and
so to England. He was home again in August 1639,
having been absent in all fifteen or sixteen months.
Milton's Continental tour, and especially the Italian
portion of it, remained one of the chief pleasures of hia
memory through all his subsequent life. Nor was it quite
without fruits of a literary kind. Besides two of his Latin
EpUtolss Familiares, one to the Florentine grammarian
Buommattei, and the other to Lucas Holstenius, there
have to be assigned to Milton's sixteen months on the
Continent his three Latin epigrams Ad Leonoram Eomie
Canentem, his Latin scazons Ad Salsillum Poetam
Momanum jEgrotantem, his fine and valuable poem in
Latin hexameters entitled Mansus, and his Five Italian
Sonnets, with a Canzone, celebrating the channs of some
Italian lady he had met in his travels.
''One sad and marring memory did mingle itself with all
that was otherwise so delightful in his Italian reminisceiiceB.
His bosom friend and companion from boyhood, the half-
Italian Charles Diodati, who had been to him as Jonathan
to David, and into whose ear he had hoped to pour the
whole narrative of what he had seen and done abroad, had
died during his absence. He had died, in Blackfriars,
London, in August 1638, not four months after Milton
had gone away on his tour. The intelligence had not
reached MO ton till some months afterwards, probably not
till his second stay in Florence; and,-though he must have
learnt some of the particulars from the youth's uncle in
Geneva, he did not know them fully till his return to
England. How profoundly thsy affected him appears
from his Epitaphium Damonis, then written in memory o'.
his dead friend. The importance of this poem in MUton's
biography cannot be overrated. It is perhaps the noblest
of aU his Latin poems; and, though in the form of a
pastoral, and even of a pastoral of the most artificial sort,
it is unmistakably an outburst of the most passional,'
personal grief. In this respect Lycidas, artistically perfect
though that poem is, cannot be compared with it ; and it ia
only the fact thaXLycidas is in English, while the Epitaphium
Damonis is in Latin, that has led to the notion that Edward
King of Christ's College was peculiarly and pre-eminently
the friend of Milton in his youth and early manhood.
That Milton, now in his thirty-first year, had been gird-
ing himself for some greater achievement in poetry than any
he had yet attempted, Cormcs not excepted, we should have
known otherwise. What we should not have kno^vn, but
for an incidental passage in the Epitaphium- Damonis, is
that, at the time of his return from Italy, he had chosen a
subject for such a high literary effort of a new Miltonic
sort. The passage is one in which, after referring to the
hopes of Diodati's medical career as so suddenly cut short
by his death, Milton speaks of himself as the sun'ivor and
of his own projects in his profefssion of literature. In
translation, it may run thus :-
" I have a theme of the TrojaDS cruising onr southern headlands
Shaping to song, and the realm of Imogen, daughter of Pandraa,
Brennus and Arvirach, dukes, and Bren'a bold brother, Belinufl ;
Then the Armoriean settlers under the laws of the Britons,
Ay, and the womb of Igraine fatally pregnant with Arthur,
Uther's son, whom he got disguised in Gorlois' likeness.
All by Merlin's craft. 0 then, if life shall be spared me,
Thou shalt be hung, my pipe, tar off on some dying old pin(-tm.
328
MILTON
Mucli-forgotton of me ; or else }roar Latian music
Changed for the British war-screech I What then I For one to
do all things,
One to hone all things, fits not t Prize sufficiently ample
Mine, and distinction great (unhoard-of ever thereafter
Thougli I should be and inglorious all through the worla of the
stranger),
li but the yellow-haired Ouse shall read me, the drinker of Alan,
Humber, which whirls as it flows, and Trent's whole valley of
orchards,
Thames, my own Thames, above all, and Tamar's western waters.
Tawny with ores, and where the wldte waves swinge the far
Orknevs. "
Interpreted prosaically, this means tnat Milton was
meditating an epic of wkich King Ai'tliur was to be the
central figure, but which should include somehow the
whole cycle of British and Arthurian legend, and that not
only was this epic to be in English, but he had resolved
that all his poetry for the future should be in the same
Not long alter Milton's return the house at Horton
ceased to be the family home. Christopher Milton and
his wife went to reside at Reading, taking the old
gentleman with them, while Milton himself preferred
London. He had first taken lodgings in St Bride's
Churchyard, at the foot of Fleet Street ; but, after a while,
probably early in 1640, he removed to a "pretty garden
house " of his own, at the end of ■ an entry, in the part of
Aldersgato Street which lies immediately on the city side
of what is now Maidenhead Court. His sister, whose
first husband had died in 1631, had married a Mr Thomas
Agar, his successor in the Crown Office ; and it was arranged
that her two sons by her first husband should be educated
by their uncle. John PhilUps, the younger of them, only
nine years old, had boarded with him in the St Bride's
Churchyard lodgings ; and, after the removal to Aldersgate
Street, the other brother, Edward Phillips, only a year
older, became his boarder also. Gradually a few other
boys, the sons of well-to-do personal friends, joined the
two Piiillipses, whether as boarders or for daily lessons,
so that the house in Aldersgate Street became a small
private school. The drudgery of teaching seems always
to have been liked by Milton. What meanwhile of the
great Arthurian epic? That project, we find, had been
given up, and Milton's mind was roving among many other
subjects, and balancing their capabilities. How he wavered
between Biblical subjects and keroic subjects from British
history, and how many of each kind suggested themselves
to him, one learns from a list in his own handwriting among
the Milton MSS. at Cambridge. It contains jottings of
no fewer than fiftyithree subjects from the Old Testament,
eight from the Gospels, thirty-three from British and
English history before the Conquest, and five from Scottish
history. It is curious that all or most of them are headed
or described as subjects for "tragedies," as if the epic
form had now been abandoned for the dramatic. It is
more interesting still to observe which of the subjects
fascinated Milton most. Though several of them are
sketched pretty fully, not one is sketched at such length
and so particularly as Paradise Lost. It is the first subject
on the list, and there are four separate drafts of a possible
tragedy under that title, two of them merely enumerating
the dramatis persome, but the last two indicating the plot
and the division into acts. Thus, in 1640, twenty -seven
years before Paradise Lost was given to the world, he had
put down the name on paper, and had committed himself
to the theme.
To tluise poetic dreaminga and schemings there was to
be a Ici;; interruption. The Scottish National Covenant
had led to extraordinary results. Not only were Charles
and Laud checkmated in their design of converting the
mild Episcopal system .which King James had sstablished
in Scotland into a high Laudian prelacy; but, in a
General Assembly held at Glasgow in the end of 1638,
Episcopacy had been utterly abohshed in Scotland, and
the old Presbyterian system of Knox and Melville revived.
To avenge this, and restore the Scottish bishops, Charles
had marched to the Border with an English army ; but,
met there by the Covenanting army under General
Alexander Leslie, he had not deemed it prudent to risk a
battle, and had yielded to a negotiation conceding to the
Scots all their demands. This " First Bishops' War," as
it came to be called, was begun and concluded while
Milton was abroad. About the time of his return, how-
ever, Charles had again broken with the Scots. Milton
had been watching the course of affairs since then with
close and eager interest. He had seen and partaken in
the sympathetic stir in favour of the Scots which ran
through the popular and Puritan mind of England. He
had welcomed the practical proof of this sympathy given
in thatEnglishparliamentof April 1640, called "The Short
Parliament," which Charles, in his straits for supplies against
the Scots, had reluctantly summoned at last, but was
obliged to dismiss as unmanageable. Charles had, never-
theless, with money raised somehow, entered on the
"Second Bishops' War." This time the result was
momentous indeed. The Scots, not waiting to be attacked
in their own country, took the aggressive, and invaded
England. In August 1640, after one small engagement
with a portion of Charles's army, they were in possession
of Newcastle and of all the northern English counties.
The English then had their opportunity. A treaty with
the Scots was begun, which the English Puritans, who
regarded their presence in England as the very blessing
they had been praying for, were in no haste to finish ; and,
on the 3d of November 1640, there met that parliament
which was to be famous in English history, and in the
history of the world, as " The Long Parliament."
Of the first proceedings of this parliament, including the
trial and execution of Strafford, the impeachment and
imprisonment of Laud and others, and the break-down of
the system of Thorough by miscellaneous reforms and by
guarantees for parliamentary liberty, Milton was only a
spectator. It was when the church question emerged
distinctly as the question paramount, and there had arisen
divisions in that question among those who had been
practically unardmous in matters of civil reform, that he
plu:/ged in as an active adviser. There were three parties
on the church question. There was a high-church party,
contending for Episcopacy by divine right, and for the
maintenance of English Epi.scopacy very much as it was ;
there was a middle party, defending Episcopacy on grounds
of usage and oxjiodiency, but desiring to see the powers of
bishops greatly curtailed, and a limited Episcopacy, ■w-itb
councils of presbyters round each bishop, substituted for
the existing high ICpiscopacy ; and there was the root-and
branch party, as it called itself, de.';iring the entire abolition
of Episcopacy and the reconstruction of the English
Church on something like the Scotti.sh Presbyterian model.
Since the opening of the parliament there had been a storm
of pamphlets crossing one another in the air from these
three parties. The chief manifesto of the high-church
party was a pamphlet by Joseph Hall, bishop of Exeter,
entitled HumUc lienionf trance to the High Court of
Parliament. In answer to Hall, and in representation of
tho views of the root-and-branch party, there had stepped
forth, in March 1640—11, five leading Puritan parish
ministers, the initials of whoso names, clubbed together on
the title-page of their joint production, made tho uncouth
word " SmectymnuiLs." These were Stephen Marshall,
Edmund Calaniy, Thomas Young, Matthew Newcomen,
and William Spurstow. The Thomas Young whoso name
MILTON
329
comes in the middle was no other than the Scottish
Thomas Young who had been Milton's domestic preceptor
in Bread Street. Having returned from Hamburg in
1628, he had b^en appointed to the vicarage of Stowmarket
in Suffolk, in which living he had remained ever since,
with the reputation 6f being one of the most solid and
learned Puritans among the English parish clergy. The
famous Smectymnuan pamphlet in reply to Hall was
mainly Young's. What is more interesting is that his old
pupU Jlilton was secretly in partnership vrith him and his
brother-Smectymnuans. Milton's hand is discernibla in a
portion of the original Smectymnuan pamphlet ; and he
continued to aid the Smectymnuans in their subsequent
rejoinders to Hall's defences of himself. It was more in
Milton's way, however, to appear in print independently;
and in May 1641, while the controversy between Hall and
the Smectymnuans was going on, he put forth a pamphlet
of his own. It was entitled Of Reformation tcntching
Church Discipline in England and the Causes that have
hitherto hindered it, and consisted of a review of English
ecclesiastical history, with an appeal to his countrymen to
resume that course of reformation which he considered to
have been prematurely stopped in the preceding century,
and to sweep away the last relics of papacy and prelacy.
Among all the root-and-branch pamphlets of the time it
stood out, and stands out stillj as the most thorough-going
and tremendous. It was followed by four others in rapid
succession, — to wit. Of Prelaiical Episcopacy and whether
it may be deduced from the Apostolical Times (June 1641),
Aniniadversions upon t/ie Remonstrant's Defence against
Sinectymnuus (July 1641), The Reason of Church Govern-
ment urged against Prelaty (February 1641-42), Apology
against a Pamphlet called a Modest Confutation of the
Animadversions, itc. (March 1641-42). The first of these
was directed chieily against that middle party which
advocated a limited Episcopacy, with especial reply to the
arguments of Archbishop IJssher, as the chief exponent of
the views of that party. Two of the others, as the titles
imply, belong to the Smectymnuan 'series, and were
castigations of Bishop Hall. The greatest of the four, and
the most important of all Milton's anti-Episcopal pamphlets
after the first, is that entitl d The Reason of Church
Government. It is there that Milton takes his readers
into his confidence, speaking at length of himself and his
motives in becoming a controversialist. Poetry, he declares,
was his real vocation ; it was with reluctance that he had
resolved to " leave a calm and pleasing solitariness, fed with
cheerful and confident thoughts, to embark in a troubled
sea of noises and hoarse disputes " ; but duty had left him
no option. The great poem or poems he had been meditat-
ing could wait ; and meanwhile, though in prose-polemics
he had the use only of his " left hand," that hand should
be used with all its might in the cause of his country and
of liberty.
The parliament had advanced in the root-and-branch
direction so far as to have passed a bill for the exclusion
of bishops from the House of Lords, and compelled the
king's assent to that bill, when, in August 1642, the
further struggle between Charles and his subjects took the
form of civil war. All England was then divided into the
Boyalists, supporting the king, and the Parliamentarians,
adhering to that majority of the Commons, with a
minority of the Lords, which sat on as the parliament.
While the first battles of the civil war were being fought
with varying success, this parliament, less impeded than
■when it had been full, moved on more and more rapidly
io the root-and-branch direction, till, by midsummer 1643,
the abolition of Episcopacy had been decreed, and the
question of the future non-prelatic constitution of the
Church of England referred to a synod of divines, to meet
at Westminster under parliamentary authority. Of Milton's
life through those first months of the civil war Uttle is
known. Ho remained in his house in Aldersgate Street,
teaching his nephews and other pupils ; and the only
scrap that came from his pen was the semi-jocose sonnet
bearing the title When the Assault was intended to the City.
In the summer of 1643, however, there was a great change
in the Aldersgate Street household. About the end of May,
as his nephew Edward Phillips remembered, Milton went
away on a country journey, without saying whither or for
what purpose ; and, when he returned, about a month
afterwards, it was with a young wife, and with some of
her sisters and other relatives in her company. He had,
in fact, been in the very headquarters of the king and the
Royalist army in and round Oxford ; and the bride he
brought back with him was a Mary Powell, the eldest
daughter of Richard Powell, Esq., of Forest Hill, near
Oxford. She was the third of a family of eleven sons and
daughters, of good standing, but in rather embarrassed
circumstances, and was seventeen years and four months
old, while Milton was in his thirty-fifth year. However
the marriage came about, it was a most unfortunate event.
The Powell fahiily were strongly Royalist, and the girl
herself seems to have been frivolous, unsuitable, and
stupid. Hardly were the honeymoon festivities over in
Aldersgate Street when, her sisters and other relativesl
having returned to Forest Hill and 'left her alone with heri
husband, she pined for home again and begged to- be
allowed to go back on a visit. Milton consented, on the
understanding that the visit was to be a brief one. This
seems to have been in July 1643. ■ Soon, -however, the
intimation from Forest Hill was that he need not look
ever to have his wife in his house again. The resolution
seems to have been mainly the girl's own, abetted by her
mother ; but, as the king's cause was then prospering in
the field, it is a fair conjecture that the whole of the
Powell family had repented of their sudden connexion with
so prominent a Parliamentarian and assailant of the Church
of England as Milton. While his wife was away, his old
father, who had been residing for three years ■n-ith his
younger and lawyer son at Reading, came to take up his
quarters in Aldersgate Street.
Milton's conduct under the insult of his wife's desertion
was most characteristic. Always fearl«ss and speculative,
he converted his own case into a public protest against the
existing law and theory of marriage. The Doctrine and
Discipline of Divorce Restored, to the good of both Sexes, was
the title of a pamphlet put forth by him in August 1643,
without his name, but with no effort at concealment, declar-
ing the notion of a sacramental sanctity in the marriage
relation to be a clerically invented superstition, and arguing
that inherent incompatibility of character, or contrariety
of mind, between two married persons, is a perfectly just
reason for divorce. There was no reference to his own
case, except by implication; but the boldness of the
speculation roused attention and sent a shock through
London. It was a time when the authors of heresies of
this sort, or of any sort, ran considerable risks. The
famous Westminster Assembly of Divines, called by the
Long Parliament, had met on the appointed day, July 1,
1643; the Scots, in consenting to send an army into
England to assist the parliament in theii war with the
king, had proposed, as one of the conditions, their Solemn
League and Covenant, binding the two nations to endeavour
after a uniformity of religion and of ecclesiastical discipline,
with the extirpation of all " heresy, schism, and profaiie-
ness," as well as popery and prelacy; the Solemn League and
Covenant had been enthusiastically accepted in England,
and was being sworn to universally by the ParUaraentarians;
and one immediate effect was that four eminent Scottish
XYL — 4»
330
M I L T O K"
divines and two Scottish lay commissoners were added to
the Westminster Assembly and became leaders there.
Whether Milton's divorce tract was formally discussed in
the Assembly during the first months of its sitting is
unknown ; but it is certain that the London clergy,
including not a few members of the Assembly, were then
talking about it privately with anger and execration.
That there might be no obstacle to a more public prosecu-
tion, Milton threw off the anonymous in a second and
much enlarged edition of the tract, in February 1643-44,
dedicated openly to the parliament and the Assembly.
Then, for a month or two, during which the gossip about
him and his monstrous doctrine was spreading more and
more, he turned his attention to other subjects. Among
the questions in agitation in the general ferment of opinion
brought about by the civil war was that of a reform of
the national system of education and especially of the
tmiversities. To this question Milton made a contribution
in June 1644, in a small Tract on Education., in the form
of a letter to Mr Samuel Hartlib, a German then resident
in London and interesting himself busily in all philanthropic
projects and schemes of social reform. In the very next
month, however, July 1644, he returned to the divorce
subject in a pamphlet addressed specially to the clergy
and entitled The Judgment of Martin Bucer concerning
Divorce. The outcry against him then reached its height.
He was attacked in pamphlets ; he was denounced in
pulpits all through London, and more than once in sermons
b^ore the two Houses of Parliament by prominefit divines
of the Westminster Assembly ; strenuous efforts were made
to bring him within definite parUamentary censure. In
the cabal formed against him for this purpose a leading
part was played, at the instigation of the clergy, by the
Stationers' Company of London. That company, represent-
ing the publishers and booksellers of London, had a plea
of their own against him, on the ground that his doctrine
was not only immoral, but had been put forth in an illegal
manner. His first divorce treatise, though published imme-
diately after the " Printing Ordinance " of the parliament
of June 14, 1643, requiring all pubUcatiohs to be licensed
for press by one of the official censors, and to be registered
in the books of the Stationers' Company, had been issued
without licence and without registration. Complaint to
this effect was made against Milton, with some others liable
to the same charge of conlempt of the printing ordinance,
in ?, petition of the Stationers to the House of Commons
in August 1644; and the matter came before committee
both in that House and in the Lords. It is to this
circumstance that the world owes the most popvdar and
eloquent, if not the greatest, of all Milton's prose-writings,
his famous Areopagitica, a Speech, of Mr John Jfilton
for the Liberty of Unlicensed Printing to the Parliament
of England. It appeared in the end of November 1644,
deliberately unUcensed and unregistered, as was proper
on such an occasion, and was a remonstrance addressed
to the parliament, as if in an oration to them face
to face, against their ordinance of June 1643 and the
whole system of licensing and censorship of the press.
Nobly eulogistic of the parliament in other respects, it
denounced their printing ordinance as utterly unworthy of
them, and of the new era of English liberties which they
were initiating, and called for its repeal. Though that
effect did not follow, the pamphlet virtually accomplished
its purpose. The licensing system had received its death-
blow ; and, though the Stationers returned to the charge
in another complaint to tli>) House of Lords, Milton's
offence .igainst the press ordinance was condoned. He was
still a .aUed in pamphlets, and found himself " in a world of
disestee;a " ; but he lived on through the winter of 1644-45
undisturbed in. his house in Aldersgate Street. To this
period there belong, in the shape of verse, only his sonnets
ix. and x., the first to some anonymous lid.v, and tlie
second "to the Lady Margaret Ley," with j l liaps the
Greek lines entitled Philosophus ad Eegem Qi.',uiaKt.
His divorce speculation, however, still occupied him ;
and in March 1644—45 he published simultaneously his
Tetracliordon, or Expotiiunu upon the four chief plcxa of
Scripture which treat of Marriage, and his Cotasterion, a
Reply to a nameless Answer against the Doilritie and
Discipline of Divorce. In these he repUed to Ids chief
recent assailants, lay and clerical, with mercUess severity.
It was not merely Milton's intellectual eminence thai
had saved him from prosecution for his divorce heresy. A
new tendency of national opinion on the church question
had operated in his favour, and in favour of all forms of
free speculation. There had occurred in the Westminster
Assembly itself, and more largely throughout the general
community, that split of English Puritanism into the two
opposed varieties of Presbyteriacism on the one hand and
Independency or Congregationalism on the other which
explains the whole subsequent history of the Puritan revo-
lution. Out of this theoretical discussion as to the con-
stitution of the church there had grown the all-important
practical question of toleration. The Presbyterians insisted
that the whole population of England should necessarily
belong to the one national Presbyterian Church, be com-
pelled to attend its worship, and be s-ibject to its discipline,
while the Independents demanded that, if a Presbyterian
Church should be set up as the national and state-paid
church, there should at least be liberty of dissent from it,
and toleration for those that chose to form themselves-
into separate congregations. Vehement within the West-
minster Assembly itself, the controversy had attained
wider dimensions out of doors, and had inwrought itself
in a most remarkable manner with the conduct of the war.
Orthodox Presbyterian Calvinists were still the majority
of the Puritan body ; but, in the new atmosphere of hbertj-,
there had sprung up, from secret and long -suppressed seeds
in the English mind, a wonderful variety of sects and
denominations, mingling other elements with their
Calvinism, or hardly Calvinistic at all, — most of them, it is
true, fervidly Biblical and Christian after their different
sorts, but not a few professing the most coolly inquisitive
and sceptical spirit, and pushing their speculations to
strange extremes of free-thinking. These sects, growing
more and more numerous in the large tovrns, had become
especially powerful in the English Parliamentary army.
That army had, in fact, become a marching academy of
advanced opinionists and theological debaters. Now, as all
the new Puritan sects, differing however much among
themselves, saw their existence and the perpetuity of their
tenets threatened by that .system of ecclesiastical uniformity
which the Presbyterians proposed to establish, they had,
one and all, abjured Presbyterianism, and adopted the
opposite principle of Independeticy, with its appended
principle of toleration. Hence an extraordinary conflict
of policies among those who seemed to be all Parliamen-
tarians, all united in fighting against the king. The
auxiliary Scottish army, which had come into England in
January 1643-44, and" had helped the English generals to
beat the king in the great battle of Marston Moor in July
1644, thought that he had then been almost sufficiently
beaten, and that the object of the Solemn League and
Covenant would be best attained by bringing him to such
terms as should secure an immediate Presbyterian settle-
ment and the suppression of the Independents and sectaries.
In this the chief English commanders, such as Essex and
Manchester, agreed substantially with the Scots. Cromwell,
on the other hand, who was now the recognized head cf
the army Independents, did not think that the king ha^
MILTON
331
been ou£5ciently beaten, even for the general purposes of
the war, and was resolved that tho war should be pushed
on to a point at which a Presbyterian settlement should bo
impossible without guarantees for liberty of conscience and
a toleration of non-Presbyteriajx sects. Through tho latter
part of 1644, accordingly, Milton had been ;:aved from the
penalties which his Presbyterian opponents would have
inflicted on him by this general championship of liberty of
opinion by Cromwell and the army Independents. Before
the middio of 1645 he, with others who wore on the
black ^ooks of tho Presbyterians as heretics, was safer
still. Though the parliament had voted, in January
1644-45, that the future national chui'ch of England should
be on the Presbyterian system, Cromwell and the Inde-
pendents had taken care to have the question of tolera-
tion left open ; and, within the next month or two, by
Cromwell's exertions, a .completely new face was put upon
tho war by the removal of all the chief officers that had
been in command hitherto, and the eqiiipment of the
New Model army, with Fairfax as its commander-in-chief
and Cromwell himself as lieutsmant-general. The Scots
and the stricter English Presbyterians looked on malignantly
while this army took the field, calling it an " Army of
Sectaries," and almost hoping it would be beaten. On
June 14, 1645, however, there was fought the great battle
of Naseby, utterly ruining the king at last, and leaving
only relics of his forces hero and there. Milton's position
then may be easily understood. Though his first tendency
on the . church question had been to somo form of a
Presbyterian constitution for the church, he had parted
utterly now from the Scots and Presbyterians, and become
a partisan of Independency, having no dread of " sects and
schisms," but regarding them rather as healthy signs in
the English body-poHtic. He was, indeed, himself one of
the most noted sectaries of the time, for in the lists of
.■iects drawn out by contemporary Presbyterian vn'iters
special mention is made of one small sect who were known
as MilionisU or Divorcers.
So far as Milton was concerned personally, his interest
in the divorce speculation came to an end in July or
August 1645, when, by friendly interference, a reconcilia-
tion was effected between him and his wife. The ruin of
the king's cause at Naseby had suggested to the Powells
that it might be as well for their daughter to go back to her
husband after their two years of separation. It was not,
however, in the house in Aldersgate Street that she rejoined
him, but in a larger house, which he had taken in the
adjacent street called Barbican, for the accommodation of
an increasing number of pupils.
The house in Barbican was tenanted by Milton from
about August 1645 to September or October 1647. Among
his first occupations there must have been the revision of
the proof sheets of the first edition of his collected poems.
It appeared as a tiny volume, copies of which are now very
rare, with the title Poems of Mr John Milton, both English
(ind Latin, composed at several times. The title-page gives
the date 1645, but January 1645-46 seems to have been
the exact month of the publication. The appearance of
the volume indicates that Jlilton may have been a little
tired by this time of his notoriety as a prose-polemic, and
desirous of being recognized once more in his original
character of literary man and poet. But, whether because
bis pedagogic duties now engrossed him or for other reasons,
very few new pieces were added in the Barbican to those
that the Uttle volume had thus made public. In English,
there were only the four sonnets now numbered xi.-xiv., the
firtt two entitled " On the Detraction which followed upon
my writing certain Treatises," the third "To Mr Henry
Lawes on his Airs," and the fourth "To the Religious
Memory of Mrs Catherine Thomson," together with the
powerful anti-Presbyterian invective or "tailed sonnet"'
entitled "On the New Forcers of Conscience under the
Long Parliament"; and in Latin there were only the ode
Ad Joannem Housium, the trifle called Apologvs de
Bustico et Hero, and one interesting Familitir £/nstle
addressed to his Florentine friend Carlo Dati. Some
family incidents of importance, however, appertain to this
time of residence in Barbican. Oxford having surrendered
to Fairfax in June 1646, the whole of the Powell family
had to seek refuge in London, and most of them found
shelter in Milton's house. His first child, a daughter
named Anne, was born there on the 29th of July that
year; on the 1st of January 1646-47 his father-in-law Mr
Powell died there, leaving his affairs in confusion ; and in
the following March his own father died there, at the age
of eighty-four, and was buried in the adjacent church of St
Giles, Cripplegate. For the rest, the two years in Barbican
are nearly blank in Milton's biography. The great
Revolution was still running its course. For a time
Charle.s's surrender of himself, in May 1646, to the auxiliary
Scottish army rather than to Fairfax and Cromwell, and
his residence with that Scottish army at Newcastle in
negotiation with the Scots, had given the Presbyterians
the advantage ; but, after the Scots had evacuated England
in January 1646-47, leaving Charles a captive with hi«
EngUsh subjects, and especially after the English army had
seized him at Holmby in June 1647 and undertaken the
further management of the treaty with him, the advantage
was all the other way. It was a satisfaction to Milton,
and perhaps still a protection for him, that the " Army of
Independents and Sectaries" had come to bo really the
masters of England.
From Barbican Milton removed, in September or-
October 1647, to a smaller house in that part of High
Holborn which adjoins Lincoln's Inn Fields. His Powell
relatives had now left him, and he had reduced the
number of his pupils, or perhaps kept only his two
nephews. But, though thus more at leisure, he did not
yet resume liis projected poem, but occupied himself
rather with three works of scholarly labour which he had
already for some time had on hand. One was the com-
pilation in English of a complete history of England, or
rather of Great Britain, from the earliest times ; another
was the preparation in Latin of a complete system of
divinity, dra.vra directly from the Bible ; and the third was
the collection of materials for a new Latin dictionary.
Milton had always a fondness for such labours of scholar-
ship and compilation. Of a poetical kind there is nothing
to record, during his residence in High Holborn, but an
experiment in psalm-translation, in the shape of Psalms
Ixxx.-lxxxviii. done into service-metre in April 1648, and
the Sonnet to Fairfax, written in September of the same
year. — This last connects him again with the course of
public affairs. The king, having escaped from the custody
of the army chiefs, and taken refuge in the Isle of Wight,
had been committed to closer custody there ; all negotia-
tion between him and parliament had been declared at an
end ; and the result would probably have been his deposi-
tion, but for the consequences of a secret treaty he hnd
contrived to make with the Scots. By this treaty the
Scots engaged to invade England in the king's behalf,
rescue him from the English parliament and army, and
restore him to his full royalty, while he engaged in return
to ratify the Covenant, the Presbyterian system of church
government, and all the other conclusions of tho West-
minster Assembly, throughoi^t England, and to put
down Independency and the sects. Thus, in May 1648,
began what is called the Second Civil War, consisting first
of new risings of the Royalists in' various parts of England,
and then of a conjunction of these with a great invasioa
332
MILTON
of England by a Royalist Scottish army, under the command
of the duke of Hamilton. It was all over in August
1648, when the crushing defeat of the Scottish army by
Cromwell in the three days' battle of Preston, and the
simultaneous suppression of the English Royalist insur-
rection in the south-east counties by Fairfax's siege and
capture of Colchester, left Charles at the mercy of the
victors. — Milton's Sonnet to Fairfax was a congratulation
to that general-in-chief of the parliament on his success at
Colchester, and attested the exultation of the writer over
the triumph of the Parliamentary cause. His exultation
continued through what followed. After one more dying
effort of the parliament at negotiation with Charles, the
army took the whole business on itself. The king was
brought from the Isle of Wight ; the parliament, manipu-
lated by the army officers, and purged of all members
likely to impede the army's purpose, was converted into
An instrument for that purpose ; a court of high justice
■was set up for the trial of Charles ; and on January
30, 1648-49, he was brought to the scaffold in front of
"Whitehall. By that act England became a republic,
governed, without King or House of Lords, by the persever-
ing residue or " Rump " of the recent House of Commons,
in conjunction with an executive council of state, composed
of forty-one members appointed annually by that House.
The first Englishman of mark out of parliament to
attach himself openly to the new republic was John
Mlton. This he did by the publication of his pamphlet
entitled Tenure of Kings and Magistrates, proving that it is
lawful, and hath been held so in all ages, for any who have the
power, to call to account a Tyrant or wiclced King, and,
after due conviction, to depose and put him to death, if the
ordinary Magistrate have neglected to do it. It was out
within a fortnight after the king's death, and was Milton's
Jast performance in the house in High Holborn. The chiefs
of the new republic could not but perceive the importance
of securing the services of a man who had so opportunely
and so powerfully spoken out in favour of their tremendous
act, and who was othcrmse so distinguished. In March
1648-49, accordingly, Jlilton was offered, and accepted, the
secretaiyship for foreign tongues to the council of state
of the new Commonwealth. The salary was to be £288 a
year, worth about £1000 a year now. To be near his new
duties in attendance on the council, which held its daily
sittings for the first few weeks in Derby House, close to
TVhitehall, but afterwards regidarly in Whitehall itself, he
removed at once to temporary lodgings at Charing Cross.
In the very first meetings of council which Milton attended
le must have made personal acquaintance with President
Bradshaw, Fairfax, Cromwell himself. Sir Henry Vane,
"Whitlocke, Henry Marten, Hasilrig, Sir Gilbert Pickering,
and the other chiefs of the council and the Commonwealth,
if indeed he had not known some of them before. After a
little while, for his greater convenience, official apartments
■were assigned him in Whitehall itself.
At the date of Milton's appointment to the secretaryship
he was forty years of age. His special duty was the
drafting of such letters as were sent by the council of
state, or sometimes by the Rump Parliament, to foreign
states and princes, with the examination and translation
of letters in reply, and with personal conferences, when
necessary, with the agents of foreign jxiwers in London,
and with envoys and ambassadors. As Ijatin was the
language employed in the written diplomatic documents,
his post came to be known indifferently as the sccretaryslii])
for foreign tongues or the Ijatin secretaryship. In that
post, however, his duties, more particularly at first, were
•very light in comparison with those of his official colleague,
^Ir Walter Frost, the general secretary. Foreign powers
-held aloof from the English republic as much as they could ;
and, while Mr Frost had to be present in every meeting of
the councU, keeping the minutes, and conducting all the
general correspondence, Milton's presence was required
only when some piece of foreign busi.ness did turn up.
Hence, from the first, his employment in very miscel-
laneous work. Especially, the council looked to him for
everything in the nature of literary vigilance and literary
help in the interests of the struggling Commonwealth. Ha
was employed in the examination of suspected papers, and
in interviews vi-ith their authors and printers; and he
executed several great literary commis.sions expressly
entrusted to him by the council. The first of these was
his pamphlet entitled Observations on Ormond's Articles of
Peace uith the Irish Rebels. It was published in May
1649, and was in defence of the repubUc against a
complication of Royalist intrigues and dangers in Ireland.
A passage of remarkable interest in it is one of eloquent
eulogy on Cromwell. More important still was the
Eikonol-lastes (which may be translated " Image-Smasher "),
published by Milton in October 1649, by way of
counterblast to the famous £ik-07i Basilike ("Royal
Image "), which had been in circulation in thousands of
copies since the king's death, and had become a kind cf
Bible in aU Royalist households, on the supposition that it
had been ■nTitten by the royal martyr himself. A third
piece of work was of a more laborious nature. In the
end of 1649 there appeared abroad, under the title of
Defensio Regia pro Carolo I., a Latin vindication of the
memory of Charles, vdth an attack on the English Com-
monwealth, intended for circulation on the Continent. As
it had been written, at the instance of the exiled royal
family, by Salmasius, or Claude de Saumaise, of Leyden,
then of enormous celebrity over Europe as the greatest
scholar of his age, it was regarded as a serious blow to the"
infant Commonwealth. To answer it was thought a task
worthy of Milton, and he threw his whole strength into the
performance through the year 1650, interrupting himself
only by a new and enlarged edition of his Kikonoklastes.
Not till April 1651 did the result appear ; but then the suc-
cess was prodigious. Milton's Latin Pro Populo Anglicann
Defensio, as it was called, ran at once over the British
Islands and the Continent, rousing acclamation everywhere,
and received by scholars as an annihilation of the great
Salmasius. Through the rest of 1651 the observation was
that the two agencies which had co-operated most visibly
in raising the reputation of the Commonwealth abroad
were Milton's books and Cromwell's battles. — These battles
of Cromwell, in the service of the Commonwealth he had
founded, had kept him absent from the council of state,
of which he was still a member, since shortly after the
beginning of Milton's secretaryship. For nearly a year ho
had been in Ireland, as lord lieutenant, reconquering that
country after its long rebellion ; and then, for anotlier
year, ho had been in Scotland, crushing the Royalist
commotion there round Charles 11., and annexing Scotland
to the English republic. ■ The annexation was complete on
the 3d of September 1651, when Cromwell, chasing
Charles II. and his army out of Scotland, came up with
them at Worcester and gained his crowning victory. The
Commonwealth then consisted of England, Ireland, and
Scotland, and Cromwell was its supreme chief. — Through
the eventful year 1651, it has been recently ascertained,
Milton had added to the other duties of his secretaryshi)i
that of Government journalist. Through the whole of tliat
year, if not from an earlier period, he acfcd as licenser and
superintending editor of the Mcrcuritts Politicus, a news-
paper issued twice a week, of which Mr JIarchamont
Needham was the working editor and proprietor. Milton's
hand is discernible in some of the leading articles.
About the end of 1G51 Milton left his oflScial rooms in
MILTON
333
Whitehall for a Ijpuse he had taken on the edge of St
James's Park, in -what was then called Petty France,
Westminster, but is now York Street. The house existed
till the other day, but has been pulled down. In Hilton's
time it was a villa-looking residence, with a garden, in
a neighbourhood of villas and gardens. He had now
more to do in the special work of his office, in consequence
of the increase of correspondence with foreign powers.
But he had for some time been in ailing health ; and a
dimness of eyesight which had been growing upon him
gradually for ten years had been settling rapidly, since his
labour over the answer to Salmasius, into total blindness.
Actually, before or about May 1652, when he was but in
his forty-fourth year, his blindness was total, and he could
go about only with some one to lead him. Hence a re-
arrangement of his secretarial duties. Such of these duties
as he could perform at home, or by occasional visits to the
Council Office near, he continued to perform ; but much of
the routine work was done for him by assistants, one of
them a well-known German named Weckhcrlin,' under the
superintendence of Mr John Thurloe, who had succeeded
Mr Walter Frost in the general secretaryship. Precisely
to this time of a lull in Milton's secretaryship on account
of his ill-health and blindness we have to refer his two
great companion sonnets To the Lord General Cromviell
and To Sir Henry Fane the Younger. To about the same
time, or more precisely to the interval between May and
September 1652, though the exact date Ls uncertain, we
have to refer the death of his only son, who had been born
in his official Whitehall apartments in the JIarch of the
preceding year, and the death also of his wife, just after
she had given birth to his third daughter, Deborah. With
the three children thus left him, — Anne, but six years old,
Mary, not four, and the infant Deborah, — the bUnd
widower lived on in his house in Petty France in such
desolation as can be imagined. He had recovered suffici-
ently to Resume his secretarial duties; and the total num-
ber of his dictated state letters for the single year 1652
is equal to that of all the state letters of his preceding
term of secretaryship put together. To the same year
there belong also three of has Latin Familiar Epistles.
In December 1652 there was published Joannis Philippi
A tiff U Respomio ad Apologiam Anoyiymi Cvjusdani Tene-
brionis, being a reply by Milton's younger nephew, John
Phillips, but touched up by Milton himself, to one of
several pamphlets that had ajjpeared against Milton for his
slaughter of Salmasius. The ablest and most scurrilous
of these, which had just appeared anonymously at the
Hague, with the title Jiegii Sanguinis Clamor ad Coilum
adversus Parricidas Anglicanos ("Cry of the Royal Blood
to Heaven against the Enghsh Parricides "), Milton was
reserving for his own attention at his leisure.
On the 20th of April 1653 there was Cromwell's great
act of ai-med interference by which he turned out the small
remnant of the Eump Parliament, dismissed their council
of state, and assumed the government of England, Ireland,
and Scotland into his own hands. For several months,
indeed, he acted only as interim dictator, governing by a
council of his officers, and waiting for the conclusions of
that select body of advisers which he had called together
from all parts of the country, and which the Royalists
nicknamed "The Barebones Parliament." In December
1653, however, his formal sovereignty began under the
iiame of the Protectorate, passing gradually into more than
kingship. This change from government by the Rump I
and its council to government by a single military Lord
Protector and his council was regarded by many as treason
to the republican cause, and divided those who had hitherto I
been the united Commonwealth's men into the " Pure Re- I
publicans," represented by such men as Bradshaw and Vane,
and the " Oliverians," adhering to l!io Protector. Milton,
whose boundless admiration of Cromwell had shown itself
already in his Irish tract of 1619 and in his recent sonnet,
was recognized as one of the Oliverians. He remained in
Oliver's service and was his Latin secretary through the
whole of the Protectorate. For a while, indeed, his Latin
letters to foreign states in Cromwell's name were but few, — -
Mr Thurloe, as general secretary, officiating as Oliver's
right-hand man in everything, with a ilr Philip Meadows
under him, at a salary of £200 a year, as deputy for the
blind Mr Milton in foreign correspondence and translations.
The reason for this temporary exemption of Milton from
routine duty may have been that he was then engaged on
an answer, by commission from the late Government, to
the already-mentioned pamphlet from the Hague entitled
Eegii Sanguinis Clamor. Salmasius was now dead, and
the Commonwealth was too stable to suffer from such
attacks ; but no Royalist pamphlet had appeared so able
or so venomous as this in continuation of the Salmasian
controversy. All the rather because it was in the main a
libel on ililton himself did a reply from his pen seem
necessary. It came out in May leS-l, with the title
Joannis Miltoni Angli pro Populo Anglicano Defeiisio
iSVrancfa ("Second Defence of John Milton, Englishman,
for the People of England "). It is one of the most inter-
esting of.all Milton's writings. The author of the libel to
which it replied was Dr Peter du Moulin the younger, a
naturalized French Presbj-terian minister, then moving
about in EngUsh society, close to Milton ; but, as that was
a profound secret, and the work was universally attributed
on the Continent to an Alexander Morns, a French
minister of Scottish descent, then of much oratorical
celebrity in Holland, — who had certainly managed the
printing in consultation with the now deceased Salmasius,
and had contributed some portion of the matter, — Milton
had made this Morus the responsible person and the one
object of his castigations. 'They were frightful enough.
If Salmasius had been slaughtered in the former Defensio,
Morus was murdered and gashed in this. His moral
character was blasted by exposure of his antecedents, and
he was blazoned abroad in Europe as a detected clerical
blackguard. The terrific castigation of Moms, however,
is but part of the Defensio Secunda. It contains passages
of singular autobiographical and historical value, and
includes laudatory sketches of such eminent Common-
wealth's men as Bradshaw, Fairfax, Fleetwood, Lambert,
and Overton, together mth a long panegyric on Cromwell
himself and his career, which remains to this day unap-
proached for elaboration and grandeur by any estimate of
Cromwell from any later pen. From about the date of the
publication of the Dn/ensio Secunda to the beginning of
1655 the only specially Uterary relics of Milton's hfe are
his translations of Psalms i.-viii. in different metres, done
in August 1654, his translation of Horace's Ode i. 5, done
probably about the same time, and two of his Latin
Familiar Epistles, The most active time of his secretary-
ship for Oliver was from April 1655 onwards. In that
month, in the course of a general revision of official salaries
under the Protectorate, Milton's salary of £288 a year
hitherto was reduced to £200 a year, with a kind of re-
definition of his office, recognizing it, we may say, as a
Latin secretaryship extraordinary. Mr Philip Meadows
was to continue to do all the ordinary Foreign Office work,
under Thurloe's inspection ; but Milton was to be called
in on special occasions. Hardly was the arrangement
made when a signal occasion did occur. In May 1655 all
England was horrified by the news of the massacre of the
Vaudois Protestants by the troops of Emanuele IL, duke
of Savoy and prince of Piedmont, in consequence of their
disobedience to an edict requiring them either to leave
334
MILTON
•their native valleys or to conform to the Catholic religion.
Cromwell and his council took the matter up with all their
energy ; and the burst of indignant letters on the subject
despatched in that month and the next to the duke of
Savoy himself, Louis XIV. of France, Cardinal Mazarin, the
Swiss cantons, the States-General of the United Provinces,
and the kings of Sweden and Denmark, were all by Milton.
His famous sonnet On the late 'Massacre in Piedmont was
his more private expression of feehng on the same occasion.
'This sonnet was in circulation, and the case of the Vaudois
Protestants was still occupying Cromwell, when, in August
1655, there appeared the last of Milton's great Latin
pamphlets. It was his Pro Se Defensio, in answer to an
.■elaborate self-defence which Morus had put forth on the
Continent since Milton's attack on his character, and it con-
sisted mainly of a re-exposure of that unfortunate clergy-
man. Thence, through the rest of Cromwell's Protectorate,
Milton's life was of comparatively calm tenor. He was in
much better health than usual, bearing his blindness with
•courage and cheerfulness ; ho was steadily busy with such
more important despatches to foreign powers as the Pro-
tector, then in the height of his great foreign policy, and
regarded with fear and deference by all European monarchs
and states from Gibraltar to the Baltic, chose to confide to
him ; and his house in Petty France seems to have been,
more than at any previous time since the beginning of Kia
blindness, a meeting-place for friends and visitors, and a
scene of pleasant hospitalities. The four sonnets now
numbered xix.-xxii., one of them to young Mr Lawrence,
the son of the president of Cromwell's council, and two of
the others to Cyriack Skinner, belong to this time of domestic
quiet, as do also no fewer than ten of his Latin Familiar
Epistles. His second marriage belongs to the same years,
and gleams even yet as the too brief consummation of this
happiest time in the blind man's life. The name of his
second wife was Katharine Woodcock. He married her
on the 12th of November 1656; but, after only fifteen
months, he was again a widower, by her death in childbirth
in February 1657-58. The child dying with her, only the
three daughters by the first marriage remained. The
touching sonuet which closes the series of Milton's Sonnets
is his sacred tribute to the memory on his second marriage
and to the virtues of the mfe he had so soon lost. Even
after that loss we find him still busy for Cromwell. Mr
Meadows having been sent off on diplomatic missions,
Andrew Marvell had, in September 1657, been brought in,
much to Milton's satisfaction, as his assistant or colleague
in the Latin secretaryship ; but this had by no means
relieved him from duty. Some of his greatest despatches
for Cromwell, including letters, of the highest importance,
to Louis XIV., Mazarin, and Charles Gustavus of Sweden,
belong to the year 1658.
One would like to know precisely in what personal
relations Milton and Cromwell stood to each other. There
i.-i, unfortunately, no direct record to show what Cromwell
thought of Milton ; but there is ani|iIo record of what
Milton thought of Cromwell. "Our chief of men," he
had called Cromwell in his sonnet of .M.iy XG.rl ; and the
opinion remained unchanged. Ho thought Cromwell the
greatest and best man of his generation, or of many
generations; and he regarded Cromwell's as.sumption of
tho supreme power, and hi.s retention of that power with a
sovereign title, as no real suppression of the republic, but
as absolutely nece-ssary for tho preservation of the republic,
and for tho safeguard of the Briti.sh Islands against a
return of the Stuarts. Nevertheless, under this prodigious
admiration of Cromwell, there were political doubts and
reserves. Milton was so much of a modern radical of tho
• extreme school in his own political views and sympathies
that he cannot but have been vexed by tho growing con-
servatism of Cromwell's policy through his Protectorate. To'
his grand panegj'ric on Oliver in the Defensio Secunda of
1654 he had ventured to append cautions against self-will,
over-legislation, and over-policing ; and he cannot have
thought that OUver had been immaculate in these respects
through the four subsequent years. The attempt to revive
an aristocracy and a House of Lords, on which Cromwell
was latterly bent, cannot have been to Milton's taste.
Above all, ^lilton dissented in loto from Cromwell's church
policy. It was Milton's fixed idea, almost his deepest
idea, that there should be no such thing as an Established
Church, or state-paid clergy, of any sort or denomination or
mixture of denomination.s, in any nation, and that, as it
had been the connexion between church and state, begun
by Constantino, that had vitiated Christianity in the world,
and kept it vitiated, so Christianity would never flourish as
it ought till there had been universal disestablishment and
disendowment of the clergy, and the propagation of the
gospel were left to the zeal of voluntary pastors, self-sup-
|)ortcd, or sujiported modestly by their flocks. He had at
one time looked to Cromwell as the likeliest man to carry
this great revolution in England. But Cromwell, after
much meditation on the subject in 1652 and 1653, had
come to the opposite conclusion. The conservation of the
Establi.shcd Church of England, in the form of a broad
union of all evangelical denominations of Christians, whether
Presbyterians, or Independents, or Baptists, or moderate
Old Anglicans, that would accept state-pay with state-
control, had been the fundamental notion of his Protec-
torate, persevered in to the end. This must have been
MUton's deepest disappointment with the Olivcrian rule.
Cromwell's death on the 3d of September 165S left the
Protectorship to his son Richard. Milton and Marvell
continued in their posts, and a number of the Foreign Office
letters of the new Protectorate were of Milton's composition.
Thinking the time fit, he also put forth, in October 1658, a
new edition of his Defensio Prima, and, early in 1659, a
new English pamphlet, entitled Treatise of Civil Power in
Ecclesiastical Causes, ventilating those notions of his as to
the separation of church and state which he bad been
obliged of late to keep to him.sclf. To Richard's
Protectorate also belongs one of Milton's Latin Familiar
Episllei. Meanwhile, though all had sccmod quiet round
Richard at first, the jealousies of the army officers left about
him by Oliver, and the conflict of political elements let
loose by Oliver's death, were preparing his downfall. In
May 1659 Richard's Protectorate was at an end. The
country had returned with pleasure to what was calleJ
"the good old cause" of pure republicanism; and the
government was in the hands of "the Restored Rump,''
consisting of the reassembled remains of that Rump Parlia-
ment which Cromwell had dissolved in 1653. To this
change, as inevitable in the circumstances, or even promis-
ing, Milton adjusted himself. The last of his known
official performances in his Latin secretaryship are two
letters in the name of William Lentlmll, as the speaker of
the restored Rump, one to the king of Sweden and one to
the king of Denmark, both dated May 15, 1659. Under
the restored Rump, if ever, he seemed to have a chance for
his notion of church-discstablishincnt ; and, accordingly, in
August 1659, he put forth, with a prefatory address to that
body, a large pamphlet entitled Considerations iovc/iin</
tlif liheliest means to remove J/iretinys out of llu Church.
Tho restored Rump had no time to attend to such matters.
They wero in struggle for their own e^dstcnco with tho
army chiefs ; and tho British Islands were in that state
of hopeless confusion and anarchy which, after passing
through a brief phase of attempted military govcrnmi. iit
(October to December 1659), and a second revival of the
purely republican or Hump government (December 1659 to
MILTON
335
iFebruary 1659-60), issued in Monk's march from Scotland,
assumption of the dictatorship in London, and recall of all
the sur\'ivors of the original Long Parliament to enlarge the
Kump to' due dimensions and assist him in further delibera-
tions. Through all this anarchy the Royalist elements had
been mustering themselves, and the drift to the restoration
of the Stuart dynasty, as the only possible or feasible con-
clusion, had become apparent. To prevent that issue, to
argue against it and fight against it to the last, was the
work to which Milton had then set himself. His dis-
establishment notion and all his other notions had been
thrown aside ; the preservation of the republic in any form,
and by any compromise of difierences within itself, had
become his one thought, and the study of practical means
to this end his most anxious occupation. In a Letter to a
Friend concerning the Ruptures of the Commonwealth,
written in October 1659, he had propounded a scheme of
a kind of dual government for reconciling the army chiefs
■with the Rump ; through the following winter, marked only
by two of his Latin Familiar Epistles, his anxiety over the
signs of the growing enthusiasm throughout the country
for the recall of Charles II. had risen to a kind of agony ;
and early in March 1659-60 his. agony found vent in a
pamphlet of the most passionate vehemence entitled Tlie
Ready and Fasy Way to Establish a Free Commonwealth,
and the Excellence thereof compared with the Inconveniences
and Dangers of readmitting Kingship in this Nation. An
abridgment of the practical substance of this pamphlet was
addressed by him to General Monk in a letter entitled The
Present Means and Brief Deliweation of a Free Common-
Tvealth. Milton's proposal was that the central governing
apparatus of the British Islands for the future should con-
sist of one indissoluble Grand Council or parliament, which
should include all the political chiefs, while there should
he a large number of provincial councils or assemblies sitting
in the great to^^■n3 for the management of local and county
affairs. The scheme, so far as the public attended to it at all,
"was received with laughter; the Royalist demonstrations were
now fervid and tumultuous; and it remained only for the new
and full parliament of two Houses which had been sum-
moned under Monk's auspices, and which is now known as
the Convention Parliament, to give effect to Monk's secret
•determination and the universal popular desire. Not even
then would Milton be silent. In Bnef Notes on a late
Sermon, published in April 1660, in reply to a Royalist dis-
course by a Dr Griffith, he made another protest against
the recall of the Stuarts, even hinting that it would be
better that Monk should become king himself ; and in the
same month he sent forth a second edition of his Ready
and Easy Way, more frantically earnest than even the
first, and containing additional passages of the most violent
denunciation of the royal family, and of prophecy of the
degradation and disaster they would bring back with them.
This was the dying effort. On the 25th of April the Con-
'vention Parliament met; on the 1st of May they resolved
imanimously that the government by King, Lords, and Com-
inons should be restored ; and on the 29th of May Charles
DLL made his triumphal entry into London. 'The chief
fcepublicans had by that time scattered themselves, and
[Milton was in hiding in an obscure part of the city.
How Milton escaped the scaffold at the Restoration is a
jinystery now, and was a mystery at the time. Actually,
[in the terrible course through the two Houses of the Con-
Tention Parliament of that Bill of Indemnity by which
the fates of the surviving regicides and of so many
others of the chief republican culprits were determined,
Milton was named for special punishment. It was voted
by the Commons that he should be taken into custody by
the sergeant-at-arms, for prosecution by the ettdiney-
on account of his EikonoklasUs and Defensio
Prima, and that all copies of those books should be called
in and burnt by the hangman. There was, however, some
powerful combination of friendly influences in his favour,
with Monk probably abetting. At all events, on the 29th
of August 1660, when the Indemnity Bill did come out
complete, with the king's assent, granting full pardon to
all for their past offences, *ith the exception oi about a
hundred persons named iff the bill itself for various degrees
of punishment, thirty-four of them for death and twenty-
six for the highest penalty short of death, Milton did not
appear as one of the exceptions on any ground or' in any
of the grades. From that moment, therefore, he could
emerge from his hiding, and go about as a free man. Not
that he was yet absolutely safe. During the ne^ two
or three months London was in excitement over the
trials of such of the excepted regicides and others as had
not succeeded in escaping abroad, and the hangings and
quarterings of ten of them ; there were several public
burnings by the hangman at the same time of Milton's
condemned pamphlets ; and the appearance of the blind
man himself in the streets, though he was legally free,
would have caused him to be mobbed and assaulted. Nay,
notwithstanding the Indemnity Bill, he was in some legal
danger to as late as December 1660. Though the special
prosecution ordered against him by the Commons had been
quashed by the subsequent Indemnity Bill, the sergeant-at-
arms had taken him into custody. Entries in the Com-
mons journals of December 17 and 19 show that Milton
complained of the sergeant-at-arms for demanding exorbi-
tant fees for his release, and that the House arranged the
matter.
Milton did not rettirn to Petty France. For the first
months after he was free he lived as closely as possible in
a house near what is now Red . Lion Square, Holborn.
Thence he removed, apparently early in 1661, to a house
in Jewin Street, in his old Aldersgate-Street and Barbican
neighbourhood.
In Jewin Street Milton remained for two or three years,
or from 1661 to 1664. They were the time of his deepest
degradation, that time of which he speaks when he tells
us how, by the Divine help, he had been able to persevere
undauntedly —
" thouc;h fallen on evil days,
On evil'days though fallen, and evil tongues,
In darkness, and with dangers compassed round,
And solitude."
The "evil days" were those of the Restoration in its"
first or Clarendonian stage, with its revenges and reactions,
its return to high Episcopacy and suppression of every
form of dissent and sectarianism, its new and shameless
royal court, its open proclamation and practice of anti-
Puritanism in morals and in literature no less than in
politics. For the main part of this world of the Restora^
tion Milton was now nothing more than an infamous
outcast, the detestable blind republican and regicide who
had, by too great clemency, been left unhanged. The
friends that adhered to him still, and came to sec him in
Jewin Street, were few in number, and chieily from the
ranks of those nonconforming denominations. Independ-
ents, Baptists, or Quakers-, who were themselves under
similar obloquy. Besides his two nephews, the faithful
Andrew Marvell, CjTiack Skinner, and some others of his
former admirers, English or foreign, we hear chiefly of a
Dr Nathan Paget, who was a physician in the Jewin-
Street neighbourhood, and of several yoimg men who would
drop in upon him by turns, partly to act as his amanuenses,
and partly for the benefit of lessons from him, — one of them
an interesting Quaker youth, named Thomas Ellwood.
With all this genuine attachment to him of a select few,
Milton could truly enough describe his condition after
y'
336
M I I. T O N
tUe Restoration as one of "solitude." Nor was this the
worst. His three daughters, on whom he ought now to
have been able principally to depend, were his most serious
domestic trouble. The poor motherless girls, the eldest in
her seventeenth year in 1662, the second in her fifteenth,
and the youngest in her eleventh, had grown up, in their
father's blindness and too great self-absorption, iil-looked-
after and but poorly educated ; and the result now
appeared. They "made nothing of neglecting him " ; they
rebelled against the drudgery of readmg to him or other-
wise attending on him ; they " did combine together and
counsel his maid-servant to cheat him in her marketings " ;
they actually "had mado away some of his books, and
would have sold the rest." It was to remedy this horrible
state of things that Milton consented to a third mar-
riage. The wife found for him was Elizabeth Minshull,
of a good Cheshire family, and a relative of Dr Paget's.
They were married on the 24th of February 1662-63, the
wife being then only in her twenty-fifth year, while MUton
was in his fifty-fifth. She proved an excellent wife ; and
the Jewm Street household, though the daughters remained
in it, must have been under better management from the
time of her entry into it. From that date Milton's circum-
stances must have been more comfortable, and his thoughts
about himself less abject, than they had been through the
two preceding years, though his feeling in the main must
have been still that of his own Samson : —
*• Now blind, disheartened, shamed, dishonoured, quelled,
To what can I be useful ? wherein serve
ITy nation, and tlie work from heaven imposed ?
But to sit idle on the household hearth,
A burdenous drone, to visitants a gaze,
Or pitied object."
Tliat might be the appearance, but it was not tne reality.
All the while of his seeming degradation he had found
Eome solace in renewed industry of various kinds among
his books and tasks of scholarship, and all the whUe, more
particularly, he had been building up his Paradise Lost.
He had begun the poem in earnest, we are told, in his
house in Petty France, in the last year of Cromwell's
Protectorate, and then not in the dramatic form contem-
plated eighteen years before, but deliberately in the epic
form. He had made but little way when there came the
interruption of the anarchy preceding the Restoration and
of the Restoration itself ; but the work had been resumed
in Jewin Street and prosecuted there steadily, by dictations
of twenty or thirty lines at a timB to whatever friendly or
hired amanuensis chanced to be at hand. Considerable
progress had been made in this way before his third
marriage ; and after that the work proceeded apace, his
nephew Edward Phillips, who was then out in the world
on his own account, looking in when he could to revise the
growing manuscript.
It was not in the house in Jewin Street, however, that
ParaJiie Lost was finished. Not very long after the third
marriage, probably in 1664, there was a removal to another
house, with a garden, not far from Jewin Street, but in a
more private portion of the same suburb. This, which
was to be the last of all Milton's London residences, was
in the part of the present BuuhLU Row which faces the
houses that conceal the London artillery-ground and was
then known as " Artillery Walk, leading to Bunhill Fields."
Here the poem was certainly finished before July 166.5;
for, when, in that month, Milton and his family, to avoid
the Great Plague of London, then beginning its fearful
ravages, went into temporary country-quarters in a cottage
in Chalfont St Giles, Buckinghamshire, about 23 miles
from London, the finished manuscript was taken with
him, in probably more than one co]jy. This wo Icarn
from his young Quaker friend, Thomas Ell wood, who had
taken the cottage for him, and who was shown one of the
manuscript' copies, and allowed to take it away with him
icr perusal, during Milton's stay at Chalfont. Why the
poem was not published immediately after his return to his
Bunhill hoase in London, on the cessation of the Great
Plague, does not distinctly appear, but may be exploined
partly by the fact that the official licenser hesitated before
granting the necessary imprimatur to a book by a man of
such notorious republican antecedents, and partly by tha
paralysis of all business in London by the Great Fire of Sep-
tember 1666. It was not till the 27th of April 1667 that
Milton concluded an agreement with a publisher for the
printing of his epic. By the agreement of that date, still
extant, Milton sold to Samuel Simmons, printer, of Alders-
gate Street, London, for £5 dovm, the promise of another^
after the sale of a first edition of thirteen hundred copie-i,
and the further promise of two additional sums of £5 each
after the sale of two more editions of the same size respec-
tively, all his copyi'ight and commercial interest in Parodist
Lost for ever. It was as if an author now were to part
with all his rights in a volume for £17, 10s. down, and a
contingency of £52, 10s. more in three equal instalments.
The poem was duly entered by Sinmions as ready
for publication in the Stationers' Registers on the 20th oi
the following August; and shortly after that date it was Out
in London as a neatly printed small quarto, with the title
Paradise Lost : A Poem written in Ten Books : By John
Milton. The publishing price was 3s., equal to about lOs.
6d. now. It is worth noting as an historical coincidence
that the poem appeared just at the time of the fall and
disgrace of Clarendon.
The effect of the publication of Paradise Lost upon
Milton's reputation can only be described adequately, as
indeed it was consciously described by himself in metaphor,
by his own words on Samson's feat of triumph over tha
Philistines : —
But he, thouG^h blind of sight,
Despised, and thought exting\iishcd quite,
With inward eyes illuminated,
His fiery virtue roused
From under ashes into sudden flame,
And as an evening dragon came.
Assailant on tlie perched roosts
And nests in order ranged
Of tame villatic fowl, but as an eagle
His cloudless thunder bolted on their heads."
As the poem circulated and found readers, whether in
the first copies sent forth by Simmons, or in subsequent
copies issued between 1667 and 1669, with varied title-
pages, and the latest of them with a prefixed prose
"Argument," the astonishment broke out everywhere.
" This man cuts us all out, and the ancients too " is the
saying attributed to Dryden on the occasion ; and it is the
more remarkable because the one objection to the pOem
which at first, we are told, " stumbled many " mustTiave
" stumbled " Drj-den most of all. Excei)t in the drama,
rhyme was then thought essential in anything professing
to be a poem ; blank verse was hardly regarded as verse at
all ; Dryden especially had been and was the champion of
rhyme, contending for it even in the drama ; and yet here
was an epic not only written in blank verse, but declaring
itself on that account to be " an example set, tho first in
English, of ancient liberty recovered to heroic -poem from
the troublesome and modern bondage of riming." That,
notwithstanding this obvious blow struck by the poem at
Dryden's pet literary theory, he should have welcomed tho
poem so enthusiastically and proclaimed its merits so
emphatically, says much at once for his critical perception
and for the generosity of his temper. An opinion pro-
claimed by the very chief of tho Restoration literature
could- not but prevail among the contemporary scholars ;
and, though execration of the blind and unhanged regicide
MILTON
337
Bad not ceased among the fteaner critics, tlie general vote
was that be had nobly redeemed himself. One conse-
quence of his renewed celebrity was that yisitors of all
ranks again sought him out for the honour of his society
and conversation. His obscure house in Artillery Walk,
Bunhill, we are told, became an attraction now, "much
more than he did desire," for the learned notabilities of
his time.
The year 1^69, when the first edition of Paradise Lost
had been completely sold out, and Milton had received his
second £5 on account of it, may be taken as the time of
the perfect recognition of his pre-eminence among the
English 'poets of his generation. He was then sixty years
of age ; and it is to about that year that the accounts that
have come down to us of his personal appearance and
habits in his later life principally refer. They describe
him as to be seen every other day led about in the streets
in the vicinity of his Bunhill residence, a slender figure, of
middle stature or a Httle less, generally dressed in a grey
cloak or overcoat, and wearing sometimes a small silver-
hilted sword, evidently in feeble health, but stiU look-
ing younger than he was, with his lightish hair, and his
fair, rather than aged or pale, complexion. He would sit
in his garden at the door of his house, in warm weather,
in the same kind of grey overcoat, "and so, as well as in
his room, received the visits of people of distinguished
parts, as well as quality." Within doors he was usually
dressed in neat black. He was a very early riser, and
very regular in the distribution of his day, spending the
first part, to his midday dinner, always in his own room,
amid his books,-, with an amanuensis to read for him and
write to his dictation. Music was always a chief part
of his afternoon and evening relaxation, whether when he
was by himself or when friends were with him. His
manner with friends and visitors was extremely courteous
and affable, with just a shade of stateliness. In free con-
[versation, either at the midday dinner, when a friend or
two happened, by rare accident, to be present, or more
habitually in the evening and at the light supper which
concluded it, he was the life and soul of the company,
from Jiis " flow of subject " and his " unaffected cheerful-
ness and civility," though with a marked tendency to the
satirical and sarcastic in his criticisms of men and things.
This tendency to the sarcastic was connected by some of
those who observed it with a pecuIlSVity of his voice or
pronunciation. " He pronounced the letter r very hard,"
Aubrey tells 'us, adding Dryden's note on the subject :
" litera caninci, the dog-letter, a certain sign of a satirical
wit." He was extremely temperate in the use of wine or
any strong liquors, at meals and at all other times ; and
when supper was over, about nine o'clock, " he smoked his
pipe and drank a glass of water, and went to bed." He
suffered much from gout, the effects of which had become
apparent in a stiffening of his hands and finger-joints, and
the recurring attacks of which in its acute form were very
painful. His favourite poets among the Greeks were
HomeV and the Tragedians, especially Euripides; among
the Latins, Virgil and Ovid ; among the English, Spenser
and Shakespeare. Among his English contemporaries, he
thought most highly of Cowley. He had ceased to attend
any church, belonged to no religious communion, and had
no religious observances in his family. His reasons for
this were a matter for curious surmise among his friends,
because of the profoundly religious character of his own
mind ; but he does not seem ever to have furnished the
explanation. The matter became of less interest perhaps
after 1669, when his three daughters ceased to reside with
him, having been sent out, at considerable expense, "to
learn some curious and ingenious sorts of manufacture that
are proper for women to learn, particularly embroideries
1«>— 14
in gold or silver." After that tne honsetold in Bunhill
consisted only of Milton, his wife, a single maid-aervant,
and the " man " or amanuensis who came in for the day. '
The remaining years of Milton's life, extending through
that part of the reign of Charles II. which figures in
English history under the name of " The Cabal Administra-
tion," were by no means unproductive. In 1669 he pub-
lished, under the title of Accedenee Commenced Grammar, a
small English compendium of Latin grammar that had
been lying among his papers. In 1670 there appeared, in
a rather handsome form, and with a prefixed portrait of
him by Faithorne, done from the life, and the. best aad
most authentic that now exists, his Hisiort, of Britain to
the Norman Conquest, being all that he had" been able to
accomplish of his intended complete history of England.
In 1671 there followed his Paradise Regained and Samson
Agonistes, bound together in one small volume, and giving
ample proof that his poetic genius had not exhausted itself
in the preceding great epic. His only publication in 1672
was a Latin digest of Eamist logic, entitled Artis Logical
Plenior Institutio, of no great value, and doubtless from
an old manuscript of his earlier days. In 1673, at a
moment when the growing political discontent with the
government of Charles II. and the conduct of his court
had burst forth in the special form of a "No- Popery"
agitation and outcry, Milton ventured on the dangerous
experiment of one more political pamphlet, in which, iindcr
the title Of True Religion, Heresy, Schism, Toleration, and
what best means may be used against the groiath of Popery^
he put forth, with a view to popular acceptance, as mild
a version as possible of his former principles on the topics
discussed. In the same year appeared the second edition
of his Minor Poems. Thus we reach the year 1674, the
last of Milton's life. One incident of that year was tlio
publication of the second edition of Paradise Lost, with
the poem rearranged as now into twelve books, instead cf
the original ten. Another was the publication of a small
volume containing 'his Latin Episiolse Familiares, together
with the ProJusionfs Oratories of his student-days at
Cambridge, — these last thrown in as a substitute for his
Latin state letters in his secretaryship for the Common-
wealth and the Protectorate, the printing of which was
stopped by order from the Foreign Office. A third publical
tion of the same year, and probably the very last thing dic-
tated by Milton, was a translation of a Latin document from
Poland relating to the recent election of the heroic John
Sobieski to the throne of that kingdom, with the title A
Declaration or Letters Patents of the Election of this present
King of Poland, John the Third. It seems to have been
out in London in August or September 1674. On the 8th
of the following November, being a Sunday, Milton died,
in his house in Bunhill, of " gout struck in," or gout-fever,
at the age of sixty-five years and eleven months. He was
buried, the next Thursday, in the church of St Giles,
Cripplegate, beside his father, a considerable concourse
attending the funeral.
Before the Restoration, Milton, what with his inlieritanoe from
his father, what with the o£Gcial income of Iiis. Lttiu secretapyship,
must have been a man of very good means indeeil. Since then,
however, various heavy losses, and the cessation of all official income,
bad greatly reduced bis estate, bo that be If fc luU £900 (worth about
or over £2700 now), besides furniture and liousehold goods. By
a word-of-mouth will, made in presence of bis brother Christopher,
he had bequeathed the whole to Ms widow, on theground that ho
had done enough already for his " undutiful " daughters, and that
there remained for them his interest in their mother's marringo
portion of £1000, which had never been paid, but which their
relatives, the Powells of Forest Hill, wi-re legally bound for, and
were now in circumstances to make good. The daughters, with
the Powells probably abetting them, went to law with the widow
to upset the will ; and the decision of the couit was that they
should receive £100 each. With the £600 tliua left, the widow,
after some further stay in London, retiied to Nantvi:i:h in her
338
native Cheshire- There, respected as a fmas membe. of a locid
Baptist congregation, she l.v.J tUl 1727, Lving survived her h^
band fifty-tSrea years By that time all the th?ee daughters wer^
builder," but left^o issueTtifs^^ontSiySt'nh^?
jinmamed. before 1691 ; and only the third. Deborah 'sur^fvedl
long as her step-mother. Havin.^ cone to Ir,.l,nT„'= •
to a lady, shortly before her fatger^s death .i?^' H '°"'l'T°''
Abraham CWke,'a silk.weaveriXwtwitlwht^Wr^ru'™^^
to London about 1684. when thev kpHIb.i ir/ »i, -u "'"'?'=''
business in S,,itamelds.Vatht%lJ^Lg%"lt rhing^in'teT:^^^^^^
though latter V some public attention was paid fo DcboraT by
Addison and otjiers, on tier father's account. 6ne of her sons Caleb
Clarke had gone out to Madras in 1703, and had died there as
•■parish-clerk of Fort George" in 1719, leivingchildren of whom
there are some faint traces to as late as' 1727, L year of Deborah™
MILTON
de.th irv.»„f f *i ..""""."s i,z/, tne year of Deborah's
death Except for the possibility of further and untraced descent
from his Incfian grandson of Milton, the direct de" nt from m"^'
orilh.,"l'"''^vu'"' g^pddaughter, Elizabeth Clarke, another
?„,-2?fi n ' ''"''^u°- .""'"S °""<^'i o- Thomas Foster a
Spitalfields weaver, but afterwards set up a small chandlert shoo
175V"noUon:Xr sh""™ .'". ^"^^''4 ^'"' ^''^ "' Islington fn
17M not long after she and her husband had received the proceeds
1^1 h^r thiTdZ L/"'"? ^°' 7.''^ ?' J°'"'=°" fo^ her'^Senefit
^1 ner children had predeceased her, leavin" no i^smb Ar,r,„ •
brother Christopher, ^^ho had always 'been^n the ZoVe sidrin
poll ics, rose to the questionable honour of a judgeship and kntht
£ood m the latter part of the reign of James Tl He had then
become a Roman (5atbolic,-whic1i religion he proffssed till h's
t taJTeable rZV '^'-1* T '''' D-cen'^i^n " ftom ht
^ 1, ™ J good way into the 18th century. -Milton's two
nephe.vsandnup.ls Edward and John Phillips, both of hem known
^ busy and clever hack-authors before their uncle's death continued
tt?„rb""";°^ ^''^ authorship, most industrious y and variously
though not very prosperously, through the rest of their lives Edward
in a more reputable manner than jShn, and with more of endurkl
a^.giance to the rnemory of his uncle. Edward died about 1695^
Joan was ahve tdl 1706. Their half-3i<iter Ar,ni„ .v, ,'
^ughter of Milton's sister by her'^ecoTrh'ufb^andf faS Zuti I
^^^ne^FCifZs'i fl^Xg^o7St'h^reT=>r '' tT'^ i
the poet's father is in this Agar S?e branch ortheMiS ""^
Of naassesofmanuscriptthatbadbeenleftby Milton, somoporHons
saw the light posthumously. Prevented, in the last yearof h"s
life as has been mentioned, from publishing his Latin SMe zlllTs
m the same volume with his L:itm Fa,Riliar Emst/^ hXt if
-^tted the charge of the St.tc Lelta-s, pr^n^'dffr'ttprt' ogeT;
JJoclrmt, to a young Cambndge scholar, Daniel Skinner who had
been among tKe last of his amanuenses, and had, in fact been
employed Vh.m specially in copying out and arranging those two
important MSS. ffegotiations were^ foot, after i?i' tfn's deatl
between this Dan e Skinner and the Amsterdam printer Daniei
Ekevir, for the publication of both MSS., when the EngHh Govern
inent mterferei, and the MSS. were sent back by Ekevir and
tiircwn aside, as dangerous rubbish, in a cupboard in the 'sfile
RtTw^o^had ^^^-"■'"1". i° 1"6. " London' boSksSe. named
R t, who had somehow got into his possession a less perfect but
3b^l tolerably complete, copy of t\.^ SlaU UlUr,, ha'd brough
JNo other posthumous publication of Milton's apueared till IfiSi
ti: Uh''" rr""''^"' P"' f""'' " alight tTtentm'ei'j);
I)tmncs, consisting of a pa^e or two, of rather dubious authen-
t.city said to have been withheld from his mstory of BrUainl,
f^l^T; W ^" ",?^ appeared ^ Bri,f U^lory of MoTaZ.
and of other less-known Countries hinn eastward nf R,,7jy
far as Catkay,. ndouUeiU MUton'sf^'nd^ ^^ cin^n oHL:
prose eompUations with wtich he sometimes occupied his eisnre
swelled to three folio volumes of MS., all that is known is that
r» 1 ■ L — ; .v^.u.woa ui iiio. ail mat IS known is that
after having been used by Edward Phillips for someof Awpedagog ^
books, they came into the hands of a comicittce of dmbfhfo^
scholars and wore use<i for that Latin dictionary of 1693, called rf^
€amb,-tdg,V^^onary, on which Ainsworth's'i),WWry and al
subsequent Latin dictionaries of English manufacture have been
^i a: '"V^'^r ^h'" ""' P»l'li'''='=d in three folio volumes under
the editorship of John Toland, the first collecrive edition of Milton's
prose works, rrofessing to have been printed at Amsterdam Ihoueh
really printed in London. A very interesring folio volume nul^
I.6hed in 1743 by "Joha NickoUs, junior,'? under To ti.fe of
.^'■"l" , ' ^"^ f"^'" "•^'^'"" addressed to Oliver Cromwell
lonsiats of a number of lutimato Cromwcllian documents that had
5r,t 7"'^ ■n'°Milton's possession immediately ^fter Cromwell's
death, and were left by him confideatioUj to the Quaker Ellwood.
I FinaUy, a chance search in the London State Paper Office in irm
»nV!-^°T^"°.S' ""■" """■ "it'':^'". has seemed proper in such
an article as the present. What little of closing remark is ne«^
M on' ri°"°''v/'"'=" ',■'"' "'o °b"°»» f^<=t of the divL'oT^
^ -a ' h?tLe of"v ,"'^^?1"°? mechanically distinct p riod^'
t^^ntv ;l!r r '"s.youth and minor poems, (2) his middU
an? h''ad*'hi,°"n'?i"* '" ""' "^'° ^^^^ ^ ^'^ thirty-second year.
and had his literary remains been then coUected, he would hav.
one „fTh"°''"f "' ""^ °^ *''' ^''^ I'^«"i=t« of tis generation anJ
one of the most exquisite of minor English poets. In the latter
ciai^cter, more particulariy, he would have taken his place aaone
of that nteresting group or series of English poets, coming U, ?ha
ne.n forty years alter Spenser, who, because th^ aU acknowlSerf
a filial relationship to Spenser, may be called collectWely 'fho
noTs'oMh:- r " '^'f r"'' °/ -'■-^. ^'--ntiBg in itsuch othe^r t^^^
woi 1,1 b^vl V, Y /• ?'"'P™"°°°'l<'f "'"tbomden, MUton
lift and wb^l ™ V'l'^' ^^- "■," ?'""" <^o\ie„i\ou of pieces he hid
T'h, ^ n'T"'^ ''"'' ""Glided his Ode <m the NativUy hS
tW tt, , c^"y "."= "■">' '"«'"''' ^n-l finest. There was in Sim
that peculiar Spenserian something which might be rcardtd as the
poetic facul y in ite essence, with a closeness and perfection of v^rte!
Sr^I^mseH 1°""' '." ""^ ■""'" .SP--™n3, or even iL"tte
master himself. A very discerning critic might have gone deencr
as we can now. Few as the pieces were, and owning d.^iSo
to Spenser as the author did", he was a Spenserian wit- a dijer?
I fnHee^ r^'.''^ '\V' °7° '^"-stitution, -which prophesied, «J
, ndeed already exhibited, the passage of English poetry fvt of
TMs ifrr'"" """.' ^'i^ """ ""'Sht be called ?ho Miltonil
I en5 ° ^°»'=t'',ng, distjnguishing the new poet from other
' si*^! "d in ' "" T" ""^^ """"' perfection of literacy finish It co^
r,°m "flf °7w"'"'5'°,'"°'''^ already of the os magna sonitu.
rest 'n. !,„ "o"th formed for great utterances," that consciousnesa
frn,TrT f^ r ""=<"T.°f I'terature. "He who would not be
h,?„ f ' '"P' '° '":!"' "■'" h"eafteron laudable things ought
a ilr: A ^rfi '^''^P"'"} '^'>s MUton's own memorable expressfon
el ■ Z? / °^"" P/'-^'P'" '•'"" ^'^ '^''^" possession of him Imm Z
cailiest days; and this pnnciple of moral manliness as the trae
foundation of lugh Hterary effort, of the inextricable identity of JJ
jterary productions in kind, and their coequality in wo th, «itu
de .?t/r? "^ "" which they have their origin, might liave bin
detected, in n.ore or less definite shape, in all or most of the minor
?;?vT'".,-rU' % "'^'f^" '?™. "^ "■"* P""*' P''"«=i<; doctrine of th«
nvucbihty 0 virtue which runs tSrough his Com,,,, and whkk
IS summed up m the Jliltonic motto of the closing liui:—
" Mortals tljat would follow me.
Love Virtue : ehc alone ta fr«e.
She can teach ye how to cllmli
Higher than the Bphery chimo :
Or, II Virtue feeble were.
Heaven Itself would stoop to her."
That a yonth and early manhood of such poetical promiM ahonld
S^ri 1 ^''"''""^'"^ ^y »""■«/ yoars of all but iice^ant pro»
the author of Comus and Lyctdas, instead of keeping to the poetic
tiirmod of prose pamphleteenng on questions of church and sUte
with nothing in vei-se to glitter across the long morass but a slight
Cham of biographical and historical sonnets) Surely this i1 a
inost shallow and most unmasculine judgment. Is nothing due to
Milton s own e.vpl.inat.on of the reasons that drew him at the
jwn e.\pla _
beginning of tlio English Revolution, out"of his"lit"crary projccU and
dreamings, into active partisanship with the cause whic\i his reason
favoured ? Hear what lie says would have been the reproach of hia
own conscience to him, evening and morning, if he had abstained
from such partisanship and persisted in his poetic privacy. " Ease
and leisure was given thee for thy retired thoughu out of the .weat
of other men. Thou hadst the diligence, the parts, the langoan
of a man, if a vain subject were to be adorned or beautified- but.
when the cause of God and His church was to be pleaded, for which
purpose th.it tongue was given theo which thou hast, God listened
II Ho could hear thy voice among His zealous servants, but thou
wort dumb as a beast : from honccforwarxl he that w'lich thine own
brutish silence hath made thee." Or. if this should be in too high a
strain for the ordinary modern apprehension, may not one aak. aom
MILTON
339
amply, whether sach controtereial work as Milton did plunge
into, and persevere in for twenty years, was unworthy, after all, of
him or his powers I Do not hundreds of men, accounted among
the ablest in the world, spend their lives precisely in such work
of coutroversy on contemporary questions ; and are not some of
the men of noblest reputation in the world's history remembered
for nothing else ! If Burke, whose whole public career consisted
in a succession of speeches and pamphlets, is looked back upon
as one of the greatest men of his century on their account, why
should there be such regret over the fact that Milton, after having
been the author of Comu- and Lycidas, became for a time -the prose
orator of his earlier and more tumultuous generation ? The truth is
that it is not his exchnnge of poetry for prose oratory that is
objected to, so much as the nature of his prose oratory, the side he
took, the opinions he advocated. English scholarship and English
literary criticism have not yet sufficiently recovered from that
Inherited sycophancy to the Restoration which has covered with a
cloud the preceding twenty years of the "Great Rebellion," voting
that period of English history to be unrespectable, and all its
rhenomena of Presbyterianism, the Solemn League and Covenant,
ndependency, the sects, English republicanism, &c. , to be matters
of obsolete jargon, less worthy of attention than a Roman agrarian
law or the names of Horace's mistresses. "When this unscholarly
state o,f temper has passed, there will be less disposition to distin-
euish between Milton as the poet and Milton as the prose writer,
^hile some may recognize, with the avidity of r^ssent and partisan-
ship, tlie fact that there are in Milton's prose writings notions of
mu'cii value and consequence that have not yet been absorbed into
the English political mind, there will be a general agreement at least
as to the importance of those pamphlets historically. It will be
perceived that he was not only the greatest pamphleteer of his
generation, head and shoulders above the rest, but also that there
13 no life of that time, not even Cromwell's, in which the history
of the great Revolution in its successive phases, so far as the deep
underlying ideas and speculations were concerned, may be more
intimately and instructively studied than in Milton's. Then, on
merely literary grounds, what an interest in tlicse prose remains 1
Not only of bis Areopagitica, admired now so unreservedly because
its main doctrine has become axiomatic, but of most of his other
pamphlets, even those the doctrine of which is least popular, it may
De said confidently that they answer to his own definition of "a
^good book," by containing somehow '* the precious life-blood of a
master-spirit." From the entire series there might be a collection
of specimens, unequalled anywhere else, of the capabilities of that
older, grander, and more elaborate English prose of which the
Elizabethans and their immediate successors were not ashamed,
though it has fallen into disrepute now in comparison with the
easier and nimbler pros© which came in with Dryden. Nor will
readers -of Milton's pamphlets continue to accept the hackneyed
observation that his genius was destitute of humour. Though his
prevailing mood was the severely earnest, thero are pages in his
prose writings, both* English and Latin, of thQ most laughable
irony, reaching sometimes to outrageous farce, and some of them
as wortliy of the name of humour as anything in Swift. Here,
however, we touch on what is the worst feature in some of the prose
pamphlets, — their measureless ferocity, their boundless licence in
Scrsuual scurrility. With all allowance for the old custom of those
ays, when controversy was far more of a life-and-death business
than it is now, as well as for the intrinsic soundness of Milton's
rule of always discerning tlie ^nan behind the look^ it is impossible
for the most tolerant of modern readers to excuse Milton in this
respect to the full extent of his delinquencies.
While it is wrong to regard Milton's middle twenty years of
prose polemics as a degradation of his genius, and while the fairer
contention might bo that the youthful poet of Comus and Lycidas
actually promoted himself, and became a more powerful agency in
the world and a more interesting object in it for ever, by consent-
ing to lay aside his "singing robes " and spend a portion of his life
in great prose oratory, who does not exult in the fact that such a
life was rounded off so miraculously at the close by a final stage of
compulsory calm, when the "singing robes" could be resumed, and
Paradise Lost, Paradise Hcgained, and Samson Agonistes could issue
in succession from the blind man's chamber? Of these three
poems, and what they reveal of Milton, no need here to speak at
length. Paradise Lost is one of the few monumental works of the
world, with nothing in modern epic literature comparable to it
except the great poem of Dante. This is best perceived bv those
who penetrate beneath the beauties of the merely terrestrial portion
of the story, and who recognize the coherence and the splendour of
that vast symbolic phantasmagory by which, through the wars in
heaven inJ the subsequent revenge of the expelled archangel, it
paints forth the connexion of the whole visible universe of human
wi^ftizance and history with the grander, pre-existing, and still
environing world of the eternal and inconceivable. To this great
2^0 Paradise Rtgained is a sequel, and it ought to be read as such.
Vky legend that Milton preferred the shorter epic to the larger is
';^»Sb inconect. AU that is authentic on the subject is the state-
ment by Edward Phillips that, when it was reported to his uncle
that the shorter epic was "generally censured to bo much inferior
to the other," he "could not hear with patience any such thing."
The best critical judgment now confirms Milton's own, and pro-
nounces Paradise Eegained to be not only, within the possibilities
of its briefer theme, a worthy sequel to Paradise Lost, but also one
of the most edifying and artistically perfect poems in any language.
Finally, the poem in which Milton bade farewell to the Muse, and
in which he reverted to the dramatic form, proves that to the very
end his right hand had lost none of its power or cunning. Samson
Agonistes is the most powerful drama in our language after the
severe Greek model, and it has the additional interest of being so
contrived that, without strain at any one point, or in any one par-
ticular, of tho strictly objective incidents of the Biblical story
which it enshrines, it is yet the poet's own epitaph and his con-
densed autobiography. All in all, now that those three great
poems of Milton's later life have drawn permanently into their
company the beautiful and more simple performances of his youth
and early manhood, so that we have all his English poetry under
view at once, the )-esult has been that this mau, who would have
had to be remembered independently as the type of English magna-
nimity and political courage, is laurelled also as the supreme poet
of his nation, with the single exception of Shakespeare.
Much light is thrown upon Milton's mind in his later life, and
even upon the poems of that period, by his posthumous Latin
Treatise of Christian Doctrine. It differs from all his other prose
writings of any importance in being cool, abstract, and didactic.
Professing to bo a system of divinity derived directly from the Bible,
it is really an exposition of Milton's metaphysics and of his reasoned
opinions on all questions of philosophy, ethics, and politics. The
general effect is to show that, though he is rightly regarded as the
very genius of English Puritanism, its representative poet and
idealist, yet he was not a Puritan of what may be called the first
wave, or that wave of Calvinistic orthodoxy which broke in upon
tho absolutism of Charles and Laud, and set the English Revolu-
tion agoing. He belonged distinctly to that larger and more per-
sistent wave of Puritanism which, passing on through Inde-
pendency, included at length an endless variety of sects, many of
them rationalistic and free-thinking in the extreme, till, checked
by the straits of the Restoration, it had to contract its volume for
a while, and to reappear, so far as it could reappear at all, in the
new and milder guise of what has ever since been known as English
Liberalism. For example, the treatise shows that Milton in his
later life was not an orthodox Trinitarian, but an anti-Trinitarian
of that high Arian order, counting Sir Isaac Newton among its
subsequent English adherents, which denied the coessentiality or
coequality of Christ with absolute Deity, but regarded him as clothed
with a certain derivative divinity of a high and unfathomable kind.
It shows him also to have been Anninian, rather than Calviiiistic,
in his views of free will and predestination. It shows him to
have been no Sabbatarian, like the Puritans of the first wave,
but most strenuously anti-Sabbatarian. Indeed one of its doctrines
is that the Decaloglie is no longer the standard of human morality,
and that Christian liberty is not to be bounded by its prohibitions
or by any sacerdotal code of ethics founded on these. Hence, in
the treatise, not only a repetition of Milton's views on the mar-
riage subject and of other peculiar tenets of his that had been set
forth in his pamphlets, but some curious and minute novelties of
opinion besides. By far the most important revelation of the
treatise, however, consists in the very definite statement it makes
of Milton's metaphysical creed and of the connexion of that creed
in his mind with the revealed theology of Christianity. While,
ontologically, he starts from a pure spiritualistic theism, or from
the notion of one infinite and eteraal Spirit as the self-subsisting
God and author of all being, cosuiologically his system is that
of a pantheistic materialism, which conceive all the present uni-
verse, all that we call creation, as consisting of diverse modifications,
inanimate or animate, of one primal matter, which was originally
nothing else than an eBlux or emanation from the very substance
of God. Angels and men, no less than the brute world and the
things wo call lifeless, are formations from this one original matter,
only in higher degrees and endowed with soul and free will.
Hence any radical distinction between matter and spirit, body and
soul, is, Milton holds, fallacious. The soul of man, he holds, is
not something distinct from the body of man and capable of existing
apart, but is actually bound up with the bodily organism. There-
fore, when the body dies, the soul dies also. a=d the -sbcls xaa
ceases to exist. The immortality revealed in Scripture fs, tfiererore,
not a continued existence of the soul in an immaterial condition
immediately after death, but a miraculous revival of the whole man,
soul and body together, at the resurrection, after an intermediate
sleep. In such a resurrection, with a final judgment, a reign of
Christ, and a glorification of the saints in a new heaven and a new
earth, Milton declares his absolute belief. But, indeed, throughout
the treatise, with all its differences from the orthodox interpreta-
tions of tiie Bible, nothing is more remarkable than the profound-
ness of the reverence avowed for the Bible itself'. The very initial
340
M I L — M I L
principle of the treatise i8 that, as the Bible ia a revelation from
God of things that man could not have found out for himself, all
that the Bible says on any matter is to be accepted implicitly, in
the plain sense of the words, and without sophistication, however
strange it may seem to the natural human reason. Hence, in all
those essentials of Christianity which consist in the doctrines of
the fall of man, atonement by Christ, and restoration and sanctifica-
tion through Christ only, Milton is at one with the great body of
Christians. Altogether, what the treatise makes clear is that, while
Milton was a most fervid theist and a genuine Christian, believing in
the Bible, and valuing the Bible over all the other books in the
world, he was at the same time one of the most intrepid of English
thinkers and theologians.
For further Information reference maybe maae to Mosson'a Life of Milton
ind History of his Time, 6 vols. (1869-80), mid to lils editions of Mllion's Poedca/
iror*5(Carobildge- edition in 3 vols., 1874, and amaUer 3 vol.ed., 1882), aa M-eli as
to Todd's varioium edition of the Poetical Works, with Life (5th ed., 1852), to
Kelghtley's ii/e, Opinions, and Writings of Milton (1856). to Milton tind Seine
Zeit, by Alfred Stern (1877-79), and to Mr Mark Pattison's Milton In Mr Morley's
series of "English Writera." Collective editions of the prose works since that
of 1698 are— Symmons's (7 vols., 1806); Pickering's, with Life by Mitford (8 vols.,
prose and verse together, 1851) ; and St John's. In Bohn'a Standard Library (5
vols,, 1848-53). This iHst includes a revised edition of Bishop Sumner's transla-
tion of the Treatise of Christian J)octrine, originally published In 1825. (D. MA.)
MILWAUKEE, the largest city in the State of
Wisconsin, United States, is situated on the west shore of
Lake Michigan, 100 miles north of its southern end, 80
miles north of Chicago, and 1000 miles north-west of New
York by rail, in 43' 3' N. lat., 87° 56' W. long. (44 min.
W. of Washington). The shore of the lake is 600 fiMt
above the level of the sea.
The Milwaukee and Menomonee rivers unite in the
centre of the business portion of the city, about half a
mile from their entrance to Lake Michigan, where they ai*e
joined by a third and smaller stream^the Kinnikinnic.
A bay 6 miles from cape to cape, and 3- miles broad,
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rian of Milwaukee.
stretches in front of tliocity, which commands a fine water
view, the ground risi;ii,' along the shore 80 feet above the
level of the lake, the? gradually sloping westward to the
Milwaukee river, am' :igain rising on the west and. north
to a height of 125 ('■•n. The ground also rises to a com-
manding elevation si u:h of the valley of the Menomonee.
Few cities present io many natural attractiops of site,
as indeed its Indian name indicates (" the Beantiful hollow
or bay ") ; and art has added to nature. In the residence
parts of the city there are miles of avenues from 70 to 100
feet wide, lined on both sides with elms and maples, be-
hind which stand handsome houses with spacious lawns,
fountains, and evergreens, giving the appearance of a con-
tinuous park. The material used for building is largely
the cream-coloured brick made in the vicinity, from which
Milwaukee is sometimes called the " Cream City." The
climate, tempered by the great lake, is remarkably pleasant
and healthy. The mean temperature, as shown by the
records of twenty years, is 46°-7 Fahr. The coldest
month LB January (average 22°-37), the hottest July
(70°'4).i During the last nine years the average death-
rate has been but 20 per 1000, showing it to be one of the
healthiest of American cities. Besides a full complement
of the usual religious and charitable institutions, there \s
adjoining the city the national home for disabled United
States volunteer soldiers, consisting of several buildings
situated in grounds of 400 acres extent, which serve the
purpose of a city park. There are numerous lodges be-
longing to the freemasons and other guilds ; and the Turners'
societies, which embrace a large membership and own some
valuable buildings, have done much to create and keep up
the practice of athletic exercises among the citizens. -^Two
excellent musical societies are also established here.
Before the year 1835 Milwaukee was known only as
an Indian trading-post occupied by a Frenchman named
Solomon Juneau, who is generally spoken of as the founder
of the city. The total inhabitants in 1838 numbered only
700; in 1840 there were 1712; but in 1846 the popula-
tion amounted to 9666, in 1850 to 20,061, in 1855 to
30,118, in 1860 to 45,246, in 1870 to 71,440, and in 1880
to 115,378 (57,475 males, 58,103 females). In 1882 the
population was estimated at 130,000, — more than one
half of them of foreign parentage, a very large majority
being Germans. Notwithstanding the multitude of nation-
alities represented in the population, there are few cities
more orderly and law-abiding, the number of police
employed being less than one for every 1500 inhabitants.
Another feature worthy of mention is the large proportion
of families who own their own houses, and this is true not
only as to the mercantile and professional classes, but
especially as to the labouring population. Although the
grain trade, formerly very large here, has now greatly
diminished, the growth and prosperity of the city-have not
materially suffered, owing to the developmept of manu-
facturing industries, for which the low rents, healthy climate,
and advantageous location make it well adapted. About a
sixth of the population are engaged in the manufacture of
clothing, cigar.% cooperage, leather, bricks, sashes, doors, and
blinds, machinery, and flour (of which one million of barrels
are anniially made), and in meat-packing. Milwaukee has
become famous for its " lager beer," of which there are one
million of barrels annually produced, valued at $8,000,000.
The lake commerce is very large. The tonnage entered
and cleared in 1880 was 5,322,373 tons, being about as
large as that of Baltimore, Boston, or Philadelphia. v.The
Wisconsin Central, the Milwaukee and Lake Shore, the
Milwaukee and Northern, and the Chicago, Milwaukee,
and St Paul Bailwaj-s have their head offices here, and
the last-named, owning 4000 miles of lines, has immense
workshops in the Menomonee valley near the city.j
Milwaukee is governed by a ma)-or and a ' common
council of thirty-ninfe aldermen. '■ The streets and public
building! are under the charge of the board of pubhc works.
' The monthly aver»ge« for twenty years arc :^anuary, 22''37 ;
February, 2ri3; March, 33°-35 ; April, 43°-94 ; May, 53*76;
June, 64°-39; July, "0°04; August, 67°S»; Scptomb-r, cr.;68;
October, .48°i8j,November, 36°j27 ; December, 25".M>
M I W— M I
S4I
eompoied^f three commissioners and the city engineer, all
subject to the common council. A bountiful supply of
'water is obtained from the lake, ancf the streets are well
supplied with sewers. The value of property as assessed for
taxation was |62,0'0O,00O .in 1882,— the city debt, being
$2,500,000, mostiy, for. the water- works, which are city
property. <''
There is an efficient system of public schools under a
superintendent and board of .gchool commissioners, the
value of the buildings with their sites being estimated at
$700,000. For the higher education there are a high school,
a normal school, and three commercial colleges, while the
Eoman Catholics and Lutherans have several excellent
denominational seminaries and colleges. A public library
belonging to the city contained 20,000 volimies in
1882. (j. J.)
MIMICRY is the name given in biology to the advan-
tageous resemblance (usually protective) which one species
of animal or plant often shows to another. The word was
first applied in this metaphorical sense by Mr W. H. Bates,
'and it has since been accurately defined and limited, in its
biological application, by Mr A. JR. Wallace. Briefly put,
the essence of the phenomenon of mimicry consists in the
following relation. - A, certain species of plant or animal
possesses some special means of defence from its enemies,
such as a sting, a powerful and disagreeable odour, a
nauseous taste, or a hard integument. Some other species
inhabiting tie same district or ' a part of it, and not itself
provided with the same special means of defence, closely
resembles the first species in all external points of form
and colour, though often very different in structure and
unrrfated in the biological order. For example, a South-
American family of butterflies, the Heliconidx, are distin-
.guished by their very varied and beautiful colours, and
their slow and wetily flight; they might easily be
captured by insectivorous birds, but their remains are never
found on the ground amongst the rejected wings of other
butterflies which cover the soil in many places. They also
possess a strong pungent odour, which clings to the fingers
for many days ; and this fact led Mr Wallace to suspect
that they have a disagreeable taste, and would not there-
fore be eaten by birds after a single trial Mr Belt has
since experimentally proved the truth of that belief. But
among tiie totally distinct family of the Pieridse, most of
[which are white, there is a genus of small butterflies,
known as Leptalis, edible by birds, some species of which
are white like their allies, while the greater number exactly
resemble one. or other of the Heliconida in the peculiar
shape and colouring of their wings. As regards structure,
the two families are. widely different; yet the resemblance
of a species of one family to a species of the other is often
so close that Mi Bates and Mr Wallace, experienced
entomologists, frequently mistook them for one another at
the time of capture, arid only discovered their mistake
tipon nearer examination. Mr Bates observed several
species or varieties of Leptalis in the Amazons valley, each
of which more or less exactly copied one of the Heliconida
in its own district. Accordiiigly, they seem to be mistaken
ty birds for the uneatable insects they mimic, and so to be
benefited by their resemblance. This, which may perhaps
be regarded as the most typical instance of true mimicry,
is also the firslj to which the word was applied.
jIn considering the phenomena under review, it may. be
:well to give first the chief observed facts, which are quite
independent of any particular explanation, and then the
"^eory which has been started to account for them by Mr
Bates and Mr Wallace. Before doing so, however, true
mimicry shouU be carefully discriminated from one or
two superficially similar modes of resemblance among
crg<^c beings, whose real inyjlications are vsiy difierent.
It must not be confused with mere accidental or adaptive
resemblance, due either to simple chance or to similarity
of external condition^. As a case of the first sort, we may
adduce the real or fancied resemblance between certain
orchids and flies or spiders ; as a case of the second sort,
we may take certain African Euphorbia cese, which, growing
in dry deserts, have acquired a very close likeness to the
cactuses that cover the equally dry deserts of Mexico ; or
again the sub-Antarctic gallinaceous bird, Chionis alha,
which, living on the sea-shore, has acquired a coloration
like that of the gulls, together with the legs of a wader.
These resemblances, however, do not as such subserve any
function. The species apparently mimicking and the
species apparently mimicked either do not ii habit the
same district or do not come into any definite r Nation with
one another. The likeness is either accident !. or else it
is due to similar adaptation to similar circun 'ances. In
cases of true mimicry, on the other hand, th' laimicking
species derives a direct advantage from its Ul - iiess to the
species mimicked ; the resemblance is decepti ; and this
is equally true whether we suppose the mimii-; ;, to be pro-
duced by creative design or by natural selectioii. On either
hypothesis, however it came by its likeness, th:- mimicking
species escapes certain enemies or obtains cei ti.in sorts of
food by virtue of its resemblance to some other kind.
It should also be added that the word namicry, aa
applied to such cases, is used only in a metapL'-: ical sense.
It is not intended to imply any conscious ir voluntary
imitation' by one species of the appearance r : habits of
another. All that is meant is the fact of an r - 1 > antageons
resemblahce, a delusive similarity, which gives tli •: nimicking
animal or plant some extra protection or some s • >. cial means
of .acquiring food which it would not otherw i< have pos-
sessed but for its likeness to the creature miaiicked.
Taking animals first, mimicry does not occur very
frequently among the higher classes. In the v , tebrates it
is comparatively rare, and among mammals pi bably only
one good case has yet been adduced. Thi? is that of
Cladobaies, an insectivorous genus of the Malayan region,
many species of which closely resemble squirrel- in size, in
colour, and in the bushiness and posture of the tail. It
has been suggested by Mr Wallace (from wli mmostof
the f611owing examples have been borrowed) th; ' Cladobates
may thus be enabled to approach the insects and mall birds
which form its prey under the disguise of tlie harmless
fruit-eating squirrel. In this case, as in some others, the
resemblance is not protective, but is apparently useful to
the animal in the quest for food.
Among birds, Mr Wallace has pointed o'lt that the
general likeness of the cuckoo, a weak and defenceless
group, to the hawks and gallinaceous tribe hiakes some
approach to real mimicry. But besides such vague resem-
blances there are one or two very distinct cA-es of true
mimicry in this class of vertebrates. In A'-tralia and
the Moluccas lives a genus of duU-hued h< ley -suckers,
Trojndorhynchus, consisting of large, strong, active birds,
with powerful claws and sharp beaks. Tiiey gather
together in noisy flocks, and are very pugnacitus, driving
away crows and even hawks. In the same countries lives
a group of orioles, forming the genus Mimeta ; and these,
which are much weaker birds, have not the UoVil brilliant
colouring of their allies the golden orioles, but ;ire usually
olive-green or brown. In many cases species of Mimeta
closely resemble the Tropidorhynchi inhabiting the same
island. For example, on the island of Bouru are found
the Tropidorhynchus bouruetisis and Mimeta bourueruit,
the latter of which mimics the formei^ jn the particu-
.lars thus noted by lit Wallace : — " The tipper and under
surfaces of the two birds are exactly of the same tints of
dark and light brown. . Hie Tropidorhynckvs has a large
342
M I M I C K Y
bare black patch round the eyes ; this is copied in the
Mimeia by a patch of black feathers. The top of the head
of the Tropidorhynchus has a scaly appearance from the
narrow scale-formed feathers, which are imitated by the
broader feathers of the Mimeta having a dusky line down
each. The Tropidorhynchus has a pale ruff formed of
curious recurved feathers on the nape (which has given the
whole genus the name of friar-birds) ; this is represented in
the Mimeta by a pale band in the same position. Lastly,
the bill of the Tropidorhyru:hus is raised into a pr<;tuberant
keel at the base, and the Mimeta has the same character,
although it is not a common one in the genus. The
result is that on a superficial examination the birds
are identical, although they have important structural
differences, and cannot be placed near each other in any
natural arrangement." Allied species of Tropidorhynchus
in Ceram and Timor are similarly mimicked by the local
Mimeta of each island. Mr Osbert Salvin has Ukewise
noticed a case of mimicry among the birds of prey near
Rio Janeiro. An insect-eating hawk, Harpagus diodon, is
closely resembled by a bird-eating hawk, Accipiter pilealus.
Here the advantage seems to be that the small birds have
learned not to. fear the Harpagus, and the Accipiter is
able to trade upon the resemblance by catching them
unawares, both birds being reddish-brown when seen from
beneath. But the Accipiter has the wider range of the
two ; and where the insect-eating species is not found it
no longer resembles it, but varies in the under wing-coverts
to white. Here again the rnsprnVilance, though advantage-
ous, is not protective.
Among reptiles, Mr Wallace has instanced some curious
cases where a venomous tropical Americafa genus of snakes.
Maps, with brightly-banded colours, is closely mimicked
by several genera of harmless snakes, having no affinity
with it, but inhabiting the same region. Thus the poison-
ous Elaps fulims of Guatemala has black bands on a coral-
red grtmnd ; the harmless Plioccrus eequalis of the same
district is coloured and banded precisely like it. The
likeness affords the unarmed snakes a great protection,
because other animals probably will not touch them, mis-
taking them for the venomous kinds.
It is among the invertebrates, however, and especially
among insects, that cases of mimicry are most frequent and
were first observed. In the order Lepidoptera, besides the
classical instance of Leptalis and the Jleliconidx, a genus
of another family, the Erycinidse, also mimics the same
group. The flocks of one species of Ithomia, an uneatable
butterfly, often have flying with them a few individuals of
three other widely different genera, quite indistinguishable
from them when on the wing. In the tropics of the Old
World, the Danaidm and Acreeidic 'possess a similar protec-
tive odour, and are equally abundant in individuals ; they
are closely mimicked by various species of Papilio and
Diadema. Mr Trimen, in a paper on " Mimetic Analogies
among African Butterflies," gives a list of sixteen species or
varieties of Diadema or its allies, and ten species of Papilio,
each of which mimics a Danais or Acrica of the same
region in the minutest particulars of form and colour.
The Danais tytia of India has semi-tran.sparent bluish
wings, and a border of reddish-brown ; this coloration is
exactly reproduced in Papilio agestor and Diadema nama,
all three insects frequently coming together in collections
from Darjiling. In the Malay Archipelago the common
and beautiful Euplma midnmuf is so exactly mimicked by
two rare species of Papilio that Mr Wallace generally
mistook the latter at first for the ordinary insect. An
immense number of other instances among the Lepidoptera
have been quoted from other parts of the world.
\ Occasionally species of Lepidoptera also imitate insects
cf other orders. Many of them take on the appearance of .
bees or wasps, which are of course protected by their stings..
Thus the Sesiidse and J!geriidm, two families of diurnal
moths, have species so like hymenopterous insects that
they are known by such names as apiformis, vespiforme,
ichn,eumoniforme, sphegiforme, and so forth. The British
sesia bombiliformis closely resembles the humble bee ; the
Sphecia craboniformis is coloured like a hornet, and carries
its wings in the same fashion. Some Indian Lepidoptera
have the hind legs broad and densely hairy, so as exactly
to imitate the brush-legged bees of the same country. Mr
Belt mentions a Nicaraguan moth, Pionia lycoides, which
closely mimics a distasteful coleopterous genus, Calopteron ;
and Professor Westwood pointed out that the resemblance
to the beetle is still further increased in the moth by raised
lines of scales running lengthwise down the thorax.
Among the Coleoptera, or beetles, and other orders,
simOar disguises are not uncommon. Mr Belt noticed
species of Hemiptera and Coleoptera, as well as spiders, in
Nicaragua, which exactly resemble stinging ants, and
thus no doubt escape the attacks of birds. The genus
Calopteron is mimicked by other beetles, as well as by tku
moth Pionia. In the same country, one of the Hemiptera,
Spiniger luteicomis, has every part coloured like 'the horne^
Priocnemis, which it mimics ; " in its vibrating coloured
wing-cases it departs greatly from the normal character of
the Hemiptera, and assumes that of the hornets." Mr
Wallace mentions the longicom beetle, Cyclopeplus batesii,
which "differs totally in outward appearance from every
one of its allies, having taken upon itself the exact shape
and colouring of a globular Corynomalus, a little stinking
beetle, with clubbed antenna." Erythroplatis corallifer,
another longicom, almost exactly resembles Cephalodonta
spinipes, one of the common South-American Hispidse,
which possesses a disagreeable secretion ; and Mr Bates
also found a totally different longicom, Streptolabis
hispoides, which resembles the same insect with equal
minuteness. Some of the large tropical weevils have the
elytra so hard that they cannot be pierced by a bird's
beak ; and these are mimicked by many other comparatively
soft and eatable insects. In southern Brazil, A canthotritus
dorsalis closely resembles a Curcnlio of the hard genus
Heiliplus ; and Mr Bates found Gymnoeerus cratosomoides,
a longicorn, on the same tree with the hard weevil,
Cratosomus, which it mimics. Other beetles resemble
bees, wasps, and shielded bugs. Hairy caterpillars are
well known to be distasteful to birds, and comparatively
free from attack ; and Mr Belt found a longicorn,
Desmiphora fasciculata, covered with long brown and
black hairs, and exactly mimicking some of the short,
thick, woolly caterpillars common on the bushes around.
Amongst other orders, one of the most interesting cases
is that of certain Diptera or two-winged flies which mimic
wasps and bees. Sometimes this likeness only serves to
protect the insect from attack, by inspiring fear of a sting.
But there are also a number of parasitic flies whose larvae
feed upon the larva; of bees, as in the British genua
Voliicetla ; and these exactly mimic the bees, so that they
can enter the nests or hives to deposit their eggs without
being detected even by the bees themselves. In every
country where such flies occur they resemble the native
bees of the district. Similarly, Mr Bates found a speciea
of Mantis on the Amazons which exactly mimicked the
white ants on which it fed. On the other hand, the
defenceless species itself may mimic its persecutor, as in
the case of several crickets, Scaphura, that exactly resenible
various sand-wasps, and so escape the depredations of
those cricket-killing enemies. Another cricket from the
Philippine Islands, Condylodera triccndyloides, so closely
copies a tiger-beetle, Trieondyla, that even Professor
Westwood long retained it amoug that group in his cabinet,
MIMICRY
343
and only slowly discovered his mistake. The cases here
mentioned form but a small part of all those that have
hitherto been observed and described in the insect world.
They amount altogether to many hundreds.
Among plants, though included io the above definition
for the sake of formal completeness, instances of true
mimicry are rare or almost unknown. Perhaps the nearest
approach to this phenomenon in the vegetal world is found
in the resemblance borne by the dead-nettle, Lamium
album, and a few other labiates, to the stinging nettle,
Urtica dioica and U. urem. The true nettles are strik-
ingly protected from animal foes by their stinging hairs ;
and the general appearance of the dead-nettle is sufficiently
like them to prevent human beings from plucking it, and
therefore probably to deter herbivorous mammals from
eating it down. Mr Mansel Weale mentions another
labiate, Ajuga ophrydis, of South Africa, which closely
resembles an orchid, -and may thus induce insects to
fertilize its flowers. Mr Worthington Smith has found
three rare British fungi, each accompanying common
species which they closely resembled ; and one of the
common species possesses a bitter and nauseous taste ; so
that this would seem to be a case of true mimicry. Many
diverse instances alleged by Mr k. W. Bennett, Dr Cooke,
and others cannot be considered as genuine mimetic resem-
blances in the sense here laid down. They are mere
coincidences or similar adaptations to similar needs ; and
the word ought to be applied strictly to such likenesses
alone as benefit the organism in which they occur by caus-
ing it to be mistaken for another possessing some special
advantage of its own.
The theoretical explanation of mimicry on evolutionary principles
may best be considered in connexion with the general subject of
protective coloration and variation in form, of which it ia a very
special case. There are two ways in which imitative colouring may
benefit a species. It may help the members of the species to escape
the notice of enemies, or it may help them to deceive prey. In the
first case imitative hues enable the animal or plant to avoid being
itself devoui'ed ; in the second case they enable it to devour
others more easily, and so to secure a larger amount of food than
less deceptively coloured compeers. In the former instance we
must suppose that such indiriouals as did not possess the deceptive
colouring have been discovered and destroyed by enemies with
highly developed sight, while those which possessed it have survived.
In the latter instance we must suppose that the individuals which
have no protective colouring have failed to secure sufficient prey,
through too i-eadily betraying their presence, and that only thos«
which possessed such colouring have become the parents of future
generations. It is difficult, however, to separate these two cases,
and in mauy instances the same colouring may aid a species both
in escaping its peculiar enemies-«nd in deceiving its peculiar prey.
They may therefore most conveniently be considered together.
Colour is always liable to vary from individual to individual, as
we see in the case of domesticated fowls, rabbits, dogs, and other
animals, as well as in most cultivated flowers, wherever natural
selection cannot act to keep the tj-pical specific hues pure and true.
But in a wild state certain conspicuous colours are sure to prove
disadvantageous by betraying the individual, and these will sooner
or later get weeded out, under certain circumstances, either through
the action of enemies or by starvation resulting from the inability
to escape the notice of prey. On the other hand, certain other
colours are sure to benefit the individual by harmonizing with the
tints of the environment and these will be spared by natural
selection, so tliat the individuals possessing them will pair with
one another, and will hand down their peculiarities to their de-
scendants. In this way many species will acquire and retain a
coloration that harmonizes vpith tbeir environment as a whole or
with some special part of it. The degree to which the protective
coloration will be carried, however, must depend upon the sharp-
ness of the senses in those other organisms which it is desirable to
deceive. Large dominant herbivorous or frugivorous mammals or
binls, with relatively few enemies, would not be benefited by
protective coloration, and so they seldom exhibit it. The grasses
or fruits on which they feed cannot make any attempt to escape
them. But carnivores generally require to deceive their prey, and
therefore a large number of them exhibit marked deceptive colouring.
Still more especially ds small defeaceless birds or mammals need
to escape the notice of the carnivores, and they accordingly very
pnendly possess dull colours, because any variation in the (Urectioa
of conspicuousness is certain to be promptly cut off. Above «!!,
among insects, which are so largely the prey of birds, of reptiles,
and of other animals possessing highly developed vision, protectiva
coloration in one form or other is almost universal, except »here
a nauseous taste, hairy skin, or hard external coverings afford a
different kind of protection. In every case the weeding oat of
Ul-protected forms must depend upon the relative keenness of viaion
in the various enemies or of the prey, be they mammals, hiids,
reptiles, insects, or spiders. Hence the existence of protective
coloring and of mimicry incidenUUy affords us valuable hinia m
to the perceptive faculties of the various classes against which each
organism is thus unconsciously guarded.
Where the general aspect of the environment is most uniform,
and where little but a vague impression of colour without individual
form can be conveyed, the hues of animals are also usually uniform,
to match their surroundings, and no special imitative adaptations
of form occur. Thus, among the Arctic snows, a brown or black
animal would immediately be perceived, and if defenceless at once
devoured, while if a carnivore it would seldom or never approach
unperceived near enough to its prey to effect a capture. Hence all
such variations are at once repressed, and almost all Arctic animals,
like the American polar hare, are pure white. Elsewhere bears ai«
black or brown ; in the polar region the native species is nearly
indistinguishable from the snow in which it lives. Where the
environment undergoes a regular change from season to season the
colour of the fauna varieS with it. The Arctic fox, the ermine, the-
alpine hare, the ptarmigan and many other birds, are all more or
less brown among the brown hill-sides of autumn, and snow-white
among the ^vinter snows. Almost equally general is the sandy
colour of deserts, though this, instead of being uniform, is slightly
varied from grain to grain ; and nearly all the birds, reptiles, and
insects of Sahara exactly copy the sandy grey hue of the desert
around them. Soles and other flat-fish {PUuro;vxlidse) closalr
imitate the colour and speckled appearance of the sand on whion
they lie. The fishes and crustaceans which Inhabit the sargasso
weed are coloured the same yellow as the masses of algae to which
.tiiey cling. Aphides and many small leaf-eating caterpillars ape
bright green like the neighbouring foliage.
Where the environment is somewhat more diverge, thffresemblance
begins to show more specialized features. The lion, a large ground-
cat of desert or rocky districts, is uniformly brown ; but the tiger
and other jungle-cats have perpendicular stripes which harmonize
with the bamboos and brown grass of their native haunts ; while
the leopards, jaguars, and other iree-cats have ocellated spots which
conceal them among the mingled light and shade of the for^stsi
Large marine animals have the back black, because the water looks
dark when seen from above, but their belUes are white, so' as to.
harmonize with the colour of the surface when seen from below.
Dr Weismann has shown that most edible unprotected" caterpillare
imitate the stripes and shades of the leaves among which they feed.
Those which live upon grasses are longitudinally striped like the
blades, those which live among small leaves are spotted and varied
so as to resemble the distribution of light and shade in the bushes,
and those which live upon large veined leaves with ohliqne ribs
have oblique lines to harmonize with them. In some cases even
the unripe berries are represented on the caterpillar by small reddish
spots. A specialized form of this particular protective device is
found in the chameleon, the chameleon-shrimp, many flat-fish, and
some amphibians, all of which can vary their coloration to suit
that of the surface on which they rest. The action is reflex, and
ceases if the animal is blinded.
Where the environment is very varied, as in tropical forests, we
find the greatest variety of colouring as well as actual imitation
of particular forms ; and the protective resemblances become at
once closer and more common. Birds, reptiles, spidei-s, monkeys,
and other active predaceous creatures are constantly hunting for
insects and similar small prey amongst the fallen sticks or leaves;
and among the most powerless classes of insects only those which
very closely resemble specific objects in the environment can easily
escape them. A gradual passage can be traced from the most
general to the most special resemblances under such circumstances.
Many forestine birds nave a ground. tone of green in their plumage,
which occurs nowhere but in the tropics. Some tree-lizards are
green like the leaves oi- which they sit, others are marbled to
resemble the bark where they lie in wait for their prey. Arboreal
snakes often hang like lianas or other creepers. Insects which
cling to the trunks of trees can seldom be distinguished from the
bark. A Sumatran butterfly, Kallhna paraUtJa, always settles oii
dry bushes among dead leaves, and can then hardly be perceived
among the brown foliage, which it imitates even in the appapeat
blotches and mildew with which its wings are covered. The lamUy
of Phasmids, including the leaf and stick insects, carries sucL
forms of imitation very far indeed. Most of them are large, soft,
defenceless creatures ; but some, like PhijUium, closely resemble
green leaves, so as to be almost indistinguishable while feeding ;
and others exactly imitate short broken twigs of bamboo. Air
Wallace found one such insect, Ceroxylus lacerat'its, m BomeOa
,344
prolonged into ^in" Xfi^^ p;^bX^^kt1he'^J ""
whilfi Sir Ph.rl J TVii, f J -^ "^ singular likeness to a leaf-
Thus aororrurr* »r n !' *'™''" Phenomena somet mes occur.
Sdwithllnil '"^'^' by which it is surrounded, and
fttV'arnVre^^ltorCtTrfl^^s"""'' hide its predaceous nature
B^ow'lit' 'R,!rn" ^"divided from true mimicry by a very
^^ in t), > *'^- '*'''^'' '" ">« f'"^' t''"' some vague object
te^t^ed sne iS"r ir"™"""'"'-'^ "'"■"'»*^'^- ■"" » P-rtfcu a? t !
tectea species, as in genuine mimetic resemblance If we al^^w
however, that natural selection can produce the white colour of
Arctic animals, and the sandy hue 0/ the sole and the flounder if
L":L\Tnfect*\"ru't; "'r P"""^'^'^ totheleaVlrctl-nd
, , ,. '°=«<=t. or even to real mimicry, as in the ca«e nf tl,n
W^lrs^nitUjfeliconui^, Certain PhaLidLmTy aTfirst have
varied m the direction of green coloration, ^d these loud
oiaiscnmination in the enemies of the species At this qt^un tl,o
oidinary green P!un„nd^ would often be'lilled, while out® hoe
wh^ch tiappened to approximate rudely in the vena ion of their
Z.^f fh'^I- V"'^.""" "^'^^P" th^ sharper and mo" experienced
eyes of the birds. Thus step by sten the di,i,ni,o „„„i ?T
mo,, and mo« perfect, onIy?he'bi7protectd® ea:h gene^^Z
^vTedVnd dt::;7'G"':^th" '"^ ?°--p™'^=''""-' """'^i-
The phenomena of true mimicry may be explained bv a narallel
protection because they enable birds^eadily to discr minateThem
^d the'h r TZ'"u '''''^'- J""' '' ">^ ''^"J«d bo^; of the waT;
exc?p Cr he^m^ t Tl '7° '^ '" ^"s"' ^ toicdve bS^!
inedible kind and t^ ^f 7 most in the same direction as the
d^sll^o'^^dl'w'hile^JhV,^ s\'n^'iU^fwUrbe''',e'f?t'''""'' ^b" "'
^cirriuet '"c^Tr-?"' f' o'whr^:'i,/vrnti ,°j:
p^cktrrt-ever;Tafcr;y:'rd':pr„"'^ruhrbe'j'''"'"'.pr"
iha:?-i-tr^--33£^^^^^
of legs or antenna, and so firth The hmH "PP'^'rance
T 1-1 P resemblance in form and hue
In like manner we may explain the wneQi. «f ti,., • .•
r^cmblan™ borne by T./L//; to"th7huTbirbee 'sup^sT an
^d^ll'e" %l:-rT '"' "^r: "°^'' '' """''' "^ "t once "Kk d
the beo it „,;.v,f presented some very slight resemblance to
P" "t might manage to lay its eggs undisturbed and it. larvm
each new generation the more rfimsy distuises would be more and
-nore roaddy detected, and only those tfics which varied Zt if
MIMICRY
the direction of resembling the bees wonld snirive or kv tl,«5,
5iS& £«'•■?' ^■"~..': sS.r.L's
oiten imitate the same protected form. It al.50 accounts fnr tb.
and marvelloi^s fact to a particular case of a well-known law ^
Whatever theory be adopted, however, the facts and mo.t of
their implications remain the same . For, Whether we sunpoTe fhet
sur' ivir fT'^^'^r^ to be due to diVect creative Ts^^^^':
survival of favourable variations, it is at least clear that the dismiise
HencT^e^mlTIZ-f'^' 'i*^ 1'"^°'"' -i'nola'cdSr
imijortant. psychological im.licafions:~bn the"'h;^;(h^r':^
that the municry can never go further than
evolution, it is obvious
tho CO., f.u "'"' '•"° '""""-'.V can never so further than
wo^ d^uaVu ' ,';"'^"'"/«''"/' "''°" '^' '^'^g"^^ " advan^^S
destn ?t i/J;^ if It; and even on the hypothesis ofljecial
accu^ratethl .on !. K^ **"' '^t '""='"°" """'-l '"' niade more
Ther» t*"^ V" d be necessary for practical purposes of deception
There is much evidence in favour of this view. Mr B T L^wne"
tZZt' "■'"," ^^ --f^l'yneasured the curvature of the fceta
in the compound eyes of insects, upon which depends the minimnm
size of apprehensible objects, finds^that the mSy n the cT^f
ihe flies parasitic upon bees' nests has proceeded just so far « the
otC w^H ' )'"' '^' "°"''' ^"'^ "^ '° '■■'P^^t. ""d no furthe" In
other words, so far as measurements of an^lar distance subtended
canguide us, such a fly seems to be absolutely indistinguishable by
visbn The°nl°/'"' "7 'P'"l'' "'"■'" '''^ li-^its^f orc^nar^
h „f?' J P'-^tpres cast upon the sensorium by the fly and by i
sho ™ tw tb' ""P-^ "'°"'"'- ^^ -"^"y o*>'" ^«^s^ " ^^n bt
eves of » 1 , "™'7y ^<=™s specially intended to deceive the
SimicrvwCt^" 1 ' of animals; while there is no case of
rnimals N.fnl^i ,1^ """""J "' ^"^ '^''"^'^' "^ P'^^'s or eyeless
animals. Naturally there can be no mimicry without a creature to
deceive ; the very conception implies an external nervouT Zm
:^KmTsrL;"e''±ut1oX^ere:«mairrni5^
fngiTirariri' leYf""' r °"°"'"- . ^ -^ -iTc^^c^^!
ingiy, that it a leaf-insect is green with faint violet-brown veina
t optlTrff' «^^"y "^'.''.""ain leaf, in order to deccTv sund"
tropica birds, then those birds are capable of/perceiving the fon2
mimirr "iranv""'"^ '° *^"' P,"""''" ''^S^" ^o the^r« nceTf
^o?»r ^ r^i, ^ ^ "P ""^ f""'^ •" '° " ^°"?h "<■=' of the perceptive
powers of those creatures whom the mimicry serves to deceive Th»
exact imitation of sand and coloured pebbles in the flat-fish is a
airly safe mdicat.on that the predaceous fish by whose seJect^on
they have been developed (through the weeding out of ilbprotw ted
variations) can prettv accurately distinguish form and colour The
long green pipe fisli which cling ai^iund green sea-we^ have
sharks ^he'^wlA"';" """"« '""f '° ^"'''' ">' "^^ "f ^»»I1
cte vlikea nS^f^'^il""'/ hippocampu6 which' looks p„.
n sw 1! ? , .?' '^"^'P"* ^""^ '"'"K fucus (see figure, vol xi
p. 862), has doubtless in the same way taken on its delu ive like:
ness to the alga) among which it lives. So the cricket which
shr"ami'hu/°bv"de ""'""r ""^' have gained^uV'pretit
gestTthe probabi,fty':;'^;;h«,;x:r;':i ?;i„"':[r°[,: ■; -«;
tne wasps Ihore seems every reason to believe that in manv
instances insects, spiders, and even lizards have develo ,ed miS
or other deceptive resemblances in order 10 delude th'e eyes Tin?
sects; while in other cases the disguise hns been unconscious^
adopted to deceive fish, amphibians, 'reptile,, birds, and mammal/
Moreover, we have some grounds for 'believing that th» s^i^ of
colour ,s exceptionally strong in birds and in one or two insec
JZ?. \ ^ .l," """""^ '" "'""' ""•"'* "> have proceeded to the
Sacks of Ti*'?'"''^' animnls which are most%xposed to the
aUacks of the.sc claases. or which would find it advantageous to
deceive them. It may be added that these same ch^es m« 4e„
Sr Dl^:'inTbv ''r.'^">''"« "'" •'"?•" ^"" of "--" snd fruits oS
Mr Uarwin a hypothesis, or are at least in any case most intimatelv
ariisp^^rT^'or^'' r»°^''° ^'^"^'""^ --f "tiLr orb;::;^m^
^,To..T»r ^"'- Mimicry is thus to some extent a rough
gauge of the pcfceptive faculties of the species deceived by it
MI M — M I N
345
, 'TirfTocal mimicry which occurs among certain birds, such as
tho mocking- iHrd^ stai liug, parrot, auJ bullfinch, must of course be
placed in a w[,olly diircn-nt category from these bioKgi-ja! cases. It
is a direct rolitionat result, and it is mimicry in a literal not in a
figtirativo sense. Tho faculty seems to be due to the play-instinct
alone, and not to. subserve any directly useful function. (G. A.)
MIMNERMUS, a Greek elegiac poet, born at Smyrna,
lived about GOO B.C. His life fell in the troubled time
when the old Greek city of Smyrna was struggling to
maintain itself against the rising power of the Lydian
kings. One of the extant fragments of his poems refers
to the struggle and contrasts the jiresent effeminacy of his
countrymen with the bravery of those who had once
defeated the Lydian king Gyges. The poet mentions in
another fragment that he belonged to the stock of the
Colophonians who had seized the jEolic Smyrna. But his
most important poems were a set of elegies addressed to a
flute-player named Nanno; they were collected in twobooks
called after her name. Hermesianax mentions his love for
Nanno, and implies that it was unfortunate. Only a few
fragments of these ix)em3 have , been preserved ; and their
soft melancholy tone and delicate language give some idea
of the poet's character. His ideal is the sweet soft
luxmious Ionian life, and he would, enjoy it free from
sorrow and die as soon as he could no longer enjoy it.
Yet there is apparent some of the old stronger strain of
character which in early time raised the Ionian cities to
greatness, pride in the glories of his race and scorn for
those that are unworthy of their fathers' renown. His
experience of life was evidently sad; he felt that his
country was gradually yielding to the enemy it had once
defeated, and he knew that his own hopes were disap-
pointed. The sun himself has endless toils from rising to
setting and again from setting to rising. The life of man
is as transitory as the leaves of spring, he says, referring to
a passage in the popijar, epic poetry of Ionia (Iliad, vi.
146). He Avishes to die in his sixtieth year, a wish to
which Solon rejilied bidding him reconsider and rather
long to die when he was eighty years old. Mimnermus
was the first to make the elegiac verse, which had pre-
viously had more of the epic character, the vehicle for lore-
(Kietry, and to impart to it the colour' of his own mind.
He found the elegy devoted to objective themes ; he made
it subjective. He set his own poems to the music of the
flute, and the poet Hipponax says that he used the melan-
choly yofLo^ K/joSia?. He bears the epithet Aiyvaa-TaSi]^,
by which Solon addresses him. It is doubtful whether
this epithet is pcculiai' to himself or whether it marks him
as belonging to a musical and poetic family or school ; it
is evidently akin to the epithet Aiyeiai MoC<roi.
JIIilOSA. The Mimosex (so named from their mimicry
6i animal movements) form one of the three suborders of
'Lf^umiitiisce, and are characterized by their (usually small)
regular flowers and valvate corolla. Their 28 genera and
HOC species are aiTanged by Baillon in four series, of
which the ncjfcias (see Acacia) and the true mimosas are
the mo.-it imixjrtant. They arc distributed throughout
almost all tropical and subtropical regions, the acacias
prepoiKlerating in Austi-alia and the true mimosas in
America. The former are of considerable imi)ortance as
sources of timber, gum, and tannin, but tho latter are off
much less economic value, though a few, like the talli (.V.
ferni^iiini) of Ajabia and Central Africa, are important
treps. Most are herbs or undershrubs, but some South.
American species are tall woody climbers. Tliey are ofteS*
[ttickly. The roots of some Brazilian species are poisonou,?;
and that of Jf. pvdica, L., has irritating properties. J)/.
settsitiva has been used in America in the tr.£/itment of
fistiUa, (fcc, probably as aa astringent. The mimosas,
however, owe their interest and their extensive culti-
y»tipn, partly to the beauty of their usually bipinnate
*16— 14»
foliage, but still more to the remarkable development
in some species of the sleep movements manifested to
some extent by most of the pinnate, Zf^rMminos*, as well
as many other (especially seedling) plants. In the so-called'
" sensitive plants " these movements not only take place
under the influence of light and darkness, but can be easily,
excited by mechanical and other stimuli. When stimu-'
lated, say at the axis of one of the ' secondary petioles, the
leaflets move upwards on each side until they meet, the
movement being propagated centripetally., • It may then
be communicated to the leaflets of the other sepondary
petioles, which close (the petioles, too, converging), and
thence to the main petiole, which sinks rapidly downwards
towards the stem, the bending taking place at the pulvinus,
or swollen base of the leafstalk. See Botany, vol. iv.
p. 113, fig. 117. When shaken in any way, the leaves
close and droop simultaneously, but if the agitation be
continued, they reopen as if they had. become accus-
tomed to the shocks. • The common sensitive plant of
hot-houses is ^f. pudka, L., a native of tropical America
but now naturalized in corresponding latitudes of Asia and
Africa ; but the hardly distinguishable M. sensiliva and
others are also ■ cultivated. The common wild sensitive
plants of the United States are two species _o£ the closely
allied genus Schrankin.
MINDANAO, MINDOBO. See Philippine IslandSV
MINDEN, the chief town of a district of the same name
in Prussia, province of Westphalia, is situated about 22'
miles to the west-south-west of Hanover, on the left banlo
of the Weser, which is spanned there by two bridges. The'
older parts of the town retain an old-fashioned appearance,'
with narrow and crooked streets ; the modern suburbs
occupy the site of the former fortifications, t Tbe most
interesting building is the Roman Catholic cathedral, the
tower of which, dating from the 11th century, illustrates
the first step in the growth' of the Gothic spire in Germany.'
The nave was erected at the end of^ the 13th century, and
the choir in 1377-79. Among the other chief edifices ar^
the old church of St Martin ; the town-house, with (4
Gothic fa9ade ; the extensive courthouse ; and the Govern-)
ment offices, constructed, like many of the other buildings,'
of a iKJCuliar veined brown sandstone found in the district]
Slinden contains a gymnasium and several hospitals, besides
other charitable institutions. Its industries include linen
and cotton weaving, dyeing," calico printing, and the
manufacture of tobacco, leather, lamps, chicory, and chemi-j
cals. There is also some activity in the building of small!
craft.. In 1881 107 vessels of an aggregate burden oi
1 2,569 tons ■ entered and 'cleared the river-harbour o^
Minden. The population in 1880 was 17,869.
llinden (Mindun, Mindo), apparently a trading place of some
importance in the timeof Cliailemngne, was made the seat of abishoji'
by that monarch,, and subsequently became a flourishing member
of the Hanseatic League. In the isth century it was surrounded
with u wall. Punished by iniiitary occupation and a fine for its
reception of the Iteforniatioa in 1547, ^linden underwent similar
trials in the Thirty Years' War aud the wars of the French occupa-
tion. In 16-18 the bishopric was converted iutoa secular principality
under the elector of Brandenburg. From 1807 to 1814 Minden
•was included in the kingdom of Westphalia, and in the latter year
it passed to Prussia. In 1816 tAe fortifications, which had been
ra/ed by Frederick the Grcat after the Seven Years' AVar, were
restorcil and 6tii-ngtliei>€d, and as a fortress of the second rank it
remained tho chief military place of Westphalia down to 1872,'
when> the works wert- finally deniolished. At Tedtenli.iuscn, 3
miles to tho north of Minden, tho allied Englisli and G(g-nian troops
\inder the duke 'of Brunsn-ick gained a decisive vicf«y over the'
French in 1759.'* About 3 miles to" the soutj^of Minden is the
so-called "Porta Westfalica," a n.-nrow and picturesque defile bjj
which tho Wesfr quits the mountains and reaches the jilain. .
Mindenls not to be confoundeil with tlie Hanoverian lliiudenj
also sometimes written Minden ()iopulation 6355), at the confluence
(Miindv.i\rj) of the Werra and Fulda.
MINE. See Mininc
346
MINEK ALOGY
iPefiniri-
'miBeral.
Amor-
phoas
bodies.
OlJstalE
NATURAL objects which are homogeneous in their
mass, and in which no parts formed for special pur-
poses can be distinguished, are termed " minerals " ; and
the branch of natural science which treats of these is
termed mineralogy. Minerals difier from the structures
treated of in botany and zoology in the three following par-
ticulars. (1) They differ in the mode of their formation;
this has been accomplished, not by assimilation of matter,
producing growth from within, bat by augmentation of bulk
through accretion of particles from without. (2) Minerals
are not heterogeneous. ^Vhile the objects treated of in
ihe other departments of natural history consist of beings
possessed of life, and having parts which, being mutually
dependent, cannot be separated from one another without
a more or less complete destruction of the individual, the
objects treated of under the department of mineralogy
have so uniformly consistent an individuality that they are
not destroyed by any separation of parts, — each portion
or fragment possessing the same properties and the same
composition as the whole. And (3), while those beings
which are possessed of Ufe have their component elements
grouped into complexes, for the most part capable of more
or less freedom of motion and susceptible of change,
minerals have a constitution resulting from chemical attrac-
tions alone and an arrangement of their parts, under
physical influences, which has resulted in rigidity and an
absence of all tendency to change.
Form of Minerals — Crystallography.
The most precise definition of a mineral would be — an
' fnorganic body possessed of a definite chemical composition,
jind usually of a regular geometric form. Of these, the
second is in one respect the direct outcome of the first ;
■while many of the most important physical properties pos-
sessed by minerals are outcomes of the second.
Both the geometric form and the composition of
minerals are produced and modified under the influence of
general laws.
Mineral bodies occur in the three physical conditions of
solid, liquid, and gas. Those now found in the last two
states are few in number, and are of altogether inferior
interest to those which occur as solids ; but there is reason
to believe that the minerals we know as solids once
existed in the liquid or gaseous state, and that their pre-
sent structure was determined in the process of solidifica-
tion. All bodies thus formed may be divided into two
great classes: — -
1. Amorphous bodies, or such as do not posses.? a de-
finite and characteristic geometrical form. These (when
transparent) refract light singly in every direction (except
when under stress) : they are equally ea.sy or equally diffi-
cult to break in all directions; when broken they exhibit
a conchoidal or an earthy fracture ; they are equally hard
throughout all their parts ; they are equally elastic in all
directions ; they conduct heat with equal rapidity and in
equal amount in all directions.
2. Crystalline bodies, or such as occur in definite geo-
metrical forms bounded by flat surfaces. These present
^'.Teater facilities of separation cf their particles, or " cleav-
age," in certain directions lying in determinate planes than
they do in others ; most of them are neither equally hard
nor equally elastic in all directions, conduct heat more
rapidly in certain directions than they do in others, and,
when transparent, refract light doubly except in certain
directions.
Fig. 1.
Mineral bodies are fotmd in both of the above classes ;
and the same mineral body may occur in both the
amorphous and the crystalline condition. This is seen in
the piece of gold shown in
fig. 1, where the upper portion
has a sharply angular and a
well-defixied shape, while the
lower presents curvilinear and
rugged outlines, similar to one
another in no part. Under
favouring circumstances, it is
possible that every substance
whose composition is capable
of being represented by a
definite chemical formula —
i.e., which has an unvarying
composition — may be capable
of as.suming a definite crys-
taUine form.
Six and Form of Crystals. — They are of every size from Size of
over a yard in diameter to. mere specks requiring a high crysUta
power of the microscope to reveal their existence. Beryls
have beeu obtained in America more than 4 feet in length
by 2i in thickness, weighing 1\ tons. Equally large
crystals of apatite have been found in Canada. Thers is a
rook crystal at Milan 3J feet long by b\ in circumierence,
weighing 870 lb. The highest perfection of form, and hence
of other properties, is only found, however, in crystals of
moderate or of small size.
Variety of Form, and Constancy of Form, — The same Variety
mineral may be found in different localities, or sometimes of fon»
in the same locality, exhibiting an almost endless variety
of forms. Calc-spar occurs at a Scottish locaUty in acicu-
lar pyramidal crystals of which the length may
be ten or more times as great as the width (fig,
2) ; in tlat plates as thin as paper, in which the
length is not the hundredth part of the width ;
also in prisms, pyramids, and rhombohedra,
which at first sight (as in figs. 3, 4) seem
Fig 3
Fig. 4.
destitute of any relationship to each other. This
substance has elsewhere been noted in several
hundred forms. The minerals fluorite, pjTite,
and baryto have each been observed in over a
hundred diverse forms. Nevertheless, however
great the number, all the forms, in the case of
each mineral, may bo reduced or referred to a sing
by the simple process of examining its internal structure topareo
or the mode of arrangement ef its moleculsa. ^Thia ui^omk
Fig. i.
< typsi Roiitid
M I N?EiR A L O G Y
347
accomplished in two •n-ays^(l)by finding the ■weak joints
in that arrangement, through splitting the crystal, and
(2) by measuring the angxilar inclination of the outside
surfaces which bound the form and, from these measure-
'ments, by simple mathematical laws, arriving at what has
been termed its " primitive " or simplest form.
•oTina-tR As regards the mere recognition of a substance, such
bility of measurement in itself suffices, — the angular inclination, if
*'"'''• tho same surfaces be measured, being unvarying in each
species. It can, moreover, be shown that the possible
range of external variety of form is governed by fixed
mathematical laws, which determine precisely what crys-
talline forms are or may be produced for each species.
Comparatively few of these actually occur in nature ; but
erystallographic laws can point out the range of those
which can possibly occur, can delineate them even before
they are found, and can in all cases show the relationship
■which subsists between them and the simple or fundamental
form from which or out of which they all originate. It
must be observed that in crystalline bodies the internal
structure — that is, the arrangement of the molecules —
is as regular in an outwardly shapeless mass as in the
modelled crystal which presents itself as a perfect whole,
rroper- Definitions of Crystals, and their Members or Parts. — A
tJM anil crystal is a symmetrical sobd, either opaque or transparent,
Jmt«ls contained within surfaces which theoretically are flat, and
of a perfect polish, but which are actually frequently
curved, striated, or pitted. These surfaces are called
"planes," or "faces." The external planes of a crystal are
called its " natural planes " ; the flat surfaces obtained by
splitting a crystal are called its " cleavage planes." The
intersections of the bounding planes are called "edges,"
and planes are said to be similar ■when their corresponding
edges are proportional and their corresponding angles
equal Crystals bounded by equal and similar faces are
termed " simple forms." The cube, bounded by six equal
squares, the octahedron, bounded by eight equilateral
triangles, and the rhombohedron, bounded by six equal
rhombs, are thus simple forms. Crystals of which the
faces are not all equal and similar are termed compound
forms, or " combinations," being regarded as produced
by the union or combination of two or more simple forms.
Edges are terjned rectangular, obtuse, or acute, according
as the angle at which the faces which form the edge meet
is equal to, or greater or less than, a right angle. Edges are
similar when the planes by the intersection of which they
ere formed are respectively equal and equally incUned to
one another ; otherwise they are unlike or dissimilar,
interfer- When a figure is bounded by only one set of planes, it is
tnces. gaid to be " developed." When an edge is cut oS by a
new plane, it is said to be " replaced " ; when cut off by a
plane which f cirms an equal angle ■with each of the original
faces which formed the edge, it is said to be " truncated."
When an edge is cut off by two new faces equally inclined
to the two original faces respectively, it is said to be
" bevelled." When a solid angle is cut off by a new face
which forms equal angles ■with all the faces which went to
form the solid angle, it is said to be truncated.
Ilea, In classifying crystals and studying their properties, it
"s found convenient to introduce certain imaginary lines
•Ailed "axes." Axes are imaginary lines connecting
points in the crystal which are diametrically opposite, —
such as the centres of opposite faces, the apices of opposite
solid angles, the centres of opposite edges. Different sets
^ of axes may thus be drawn through the same crystal; but
there is always one set, usually of three, but in one special
class of crystals of four, axes, by referente to which the
geometrical and physical properties of a crystal can be
most simply explained. These axes intersect one another,
either at rieht angles, producing " orthometric " formajw
at oblique angles, producing " clinometric " forms, .'fhe
axes may be all equal, or only two equal, or all unequal
There is a definite conventional position in which for "Pn,,
purposes of description a crystal is always supposed to be tioning
held. With reference to this position one of the axes, — of cry*
that which is erect or most erect, — is termed the "verti-'*'*
cal," and the others the "lateral" The planes in which
any two of the axes lie are called the "axial" or
"diametral planes," — sometimes "sections." By these
the space around the centre is divided into "sectants."
If there are, as is generally the case, only two lateral axes,
the space is divided into eight sectants, or octants ; but, if
there are three lateral axes, it is divided into twelval
sectants.
Primitive Forms of Crystals. — If we attempt to arrive, p,i_ja
through a study of the internal structure of crystals, as tiye
evidenced by directions of weakness of cohesion, at the form*
total number of primitive or parent forms which can exist,
we find that there are thirteen such forms and no more.
Nine of these may be regarded as prisms standing upon a base,
three as octahedra standing upon a solid angle ; and there is one
twelve-sided figure, or dodecahedron.
Prisms. — Of the prisms eight have a four-sidea case. Priinnfl.
If the base is square and the prism stands erect — that is, if its
sides or lateral planes, as they are called, are perpendicular to the
base — the form is termed a " right square prism " (fig. 6). In
this the four lateral planes are rectangular and equal; they may be
either oblong or square ; in the latter case the form is the " cube "
(fig. 5). "When the base is a^ rectangle instead of a square, the
form is a "right rectangular prism' (fig. 7). In each of the
i T"''
r'i
jyj
^ d,
^
^
¥
,--•- ■•-
^
Fig. 5. Fig. 6. Fig. 7.
above three forms the edges are twelve in number. In the cubi
all the edges are equal. In the square prism the lateral edges
are all equal, but are different from the four equal edges of the
base. In the rectangular prism, two at each base differ in lengtl^
from the other two, while both differ from the lateral ; hence
there are here three sets of edges, four in each. In each of thef
three forms, however, the solid angles are eight in number, all
equal, and each enclosed by three right angles.
"When the base is a rhombus, and the prism stands erect, the form
isa *'right rhombic prism" (fig. 8). Two of the angles in the base
being here acute and two
obtuse, two of the solid
angles corresponding each
with each must differ from
the others. So also must
two of the lateral angles
be acute and two obtuse.
The four lateral faces are
equal.
When the base is a
rhomboid, and the prism stands erect, it is only the opposite
lateral faces that can be equal. The form is called a ** right
rhomboidal prism " (fig. 9). ■ -f" J \
When the base is a rhombus; but the prfsm stands obliquely on
its base, the form is called an "oblique rhombic prism " (tig. 10).^
Here the basal edges' of the lateral planes are all equal in length,;
but on account of the inclination of the prism the angles which
these edges form with the lateral edges gf the lateral planes are
two acute and two obtuse.
*'Ti
A f.
7
-n
7
Fig. 8.
Fig. 9.
Fig. 10.'^ Fig. 11. jFig. 12.
If all the edges of an oblique rhombic pHsin~are equal in length
to the breadth of the base, and if the lateral planes ar« rhombi
equal iu all respects to the basal, the form is ca'led a"rhomboJ
hedron " (fig. 11). This.ia included within six eqaal pUnes^lika
1348
MINE R A L 0 G T
Orw
the cube, bnt these pUuc3 have obliqne angles. 'I'ho rhombo-
hedron thus bears the same relation to the oblique rhombic prism
which the cube does to the right square prism- Of the eight solid
angles of a rhombohedron only two are contained by three equal
plane anglea, and these two ''apices," as they may bo called, are
opposite one another. According as the apices are acute or obtuse,
we have an acute or obtuse rhombohedron.
When the base of an oblique prism is a rhomboid, the prism
becomes an " oblique rhomboidal prism " (fig. 12). In this form,
only diagonally opposite edges are similar, as regards equality
of length and the value of the included angle. Only opposite solid
angles are equal, as are also the opposite and parallel faces.
A right prism may have an equilateral six -sided base ; it is then
called an hexagonal ]>rism." This form may be developed in two
positions relatively to each other, — one in which the transverse axes
pass from the centres of opposite faces
they pass from the centres ,■ of
13), the other in which
pposite edges of the planes
(fig. 14). The faces of the one
Bet mutually truncAte the edges
of the other. If a rhombo-
hedron be positioned so as to
rest upon one of its apices, the
faces of one hexagonal prism
would truncate the lateral i?.. i o v 1 1
edges of the rhombohedron, "S- IS. I^ig- 14.
while the faces of the other hexagonal prism would truncate its
lateral solid angles. Hexagonal prisms may be longer or shorter
than the width of their bases. 'The interfacial lateral angles are
120". The angle between the lateral and terminal faces is 90*.
Oetahedra,— The planes of these eight-faced solids are triangular,
|hed?a. and they may be regarded as made up of two four-sided pj^ramids
applied to each other, base to base. They are always positioned so
that they stand upon a solid angle with the "basal plane" — that
is, the plane which is the common base of the two pyramids — hori-
zontaL In the primitive forms now under consideration the ver-
tices of the two pyramids will in this position be vertically above
and below the centre of the base. The upper and lower solid angles
are then termed the "vertical solid angles," and the four lateral
BoHd angles are called the basal solid angles.
There are three octahedrons. In the "regular" octahedron (fig.
IB) the base is a square, and the eight faces are. equilateral triangles
of equal size. There are twelve edges, which are all equah The
faces incline to each other at an angle of 109° 28' 16", and have the
plane angles all 60°. There are six equal solid angles. When the
base of the octahedron is square, but the other edges, although
Fig. 18.
Fig, 16. Fig, 16. Fig. 17.
equal to one another, are either longer or shorter than the edges
of the base, the form is a " right square octahedron " (fig, 16).
la this the faces are isosceles triangles, the equal angles being
at the basal edge of the planes. These basal edges are equal ana
similar, but differ i* length and in angles from
the eight equal pyramidal edges. When the
base of an octahedron is a rhombus, it is called
a "right rhombic octahedron" (fig. 17).
Bodeca- ■ Dodecahedron. — This (fig, 18) has each of its
hedioQ. twelve faces a rhombus. It is, like the cube
and the octahedron, a solid which is symmetricaL
The interfacial angles are all 120°, the plane
angles are 109° 28' 16" and 70° 81' 44". The edges
aze.twenty-four, and similar. There are fourteen
Bolid angles, of which six are formed each by the meeting of four
acute piano angles, and eight by the meeting of threo obtuse ]>lane
angles.
Deter- It has been said that the above simple forms were arrived
mination at through a study of the internal structure of crystals,
of parent gjjjggy ^ disclosed by cleavage. Inasmuch, however, as
there are some minerals which cleave in only one direction,
and many which cannot be fleaved in any direction, this
method of investigation fails. Its employment, moreover,
frequently led to conflicting or embarrassing results. A
.conflicting result is when a substance has more than one
' S6t of cleavages, — that is, splits up in directions which
'.wotild result in the production of more thaa one of the
above primary or simple forms. Thus the mineral fluoritd
occurs with much the greatest frequency in the form of
the cube, and it might very consistently be held that ita
frequent occurrence in this form was a clear natural
indication that the cube was the primary or simplest form
of fluorite ; but it splits up into an octahedron. Galena
crystaUizes frequently in the form of the octahedron ; yet
to cleavage galena yields a cubic primary form. It might
be conceived that there had been, in each case, some
special tendency to assume the cubic form and the octa-
hedral form ; but one and the same piece of rock may
bear on its surface cubic crystals of fluor and octa-hedral
crystals of galena, — each of the minerals having here
assumed the primitive cleavage form of the other in pre-
ference to its own. The mineral blende crystallizes not
unfrequently in octahedra, which yield the dodecahedroa
on cleavage. Fluor crystallizes in dodecahedra, yet yields
the octahedron to cleavage. Argyrite crystallizes in cubes
and in octahedra, but yields the dodecahedron on cleavage.
Pyrite crystallizes in cubes, octahedra, and dodecahedra,
and yields both the cube and the octahedron on cleavage.
These are most embarrassing results, but they clearly
indicate so intimate a relationship to subsist between throe
of the above simple forms that it is obvious that one alone
would serve as a type form for representing the others.
The selection of that one should be based upon grounds of
most eminent simplicity, and this again is to be arrived
at by a consideration of the smallness of number of parts,
i.e., of faces, edges, and solid angles. In such a considera-
tion we find that the dodecahedron, with its higher number
of each of these, at once gives place. The cube has six
faces, the octahedron eight ; simplicity here is in favour of
the cube. The cube has twelve edges, the octahedron has
twelve ; in this respect they are equaL The cube has
eight solid angles, the octahedron six ; here the greater
simplicity is on the side of the octahedron. So that this
method of adjudicating by simplicity fails, and we are
thrown back upon the relationships which may be unfolded
through a consideration of the other elements of crystals, —
{heir axes.
Systems of Crysiala and Laws of Crystallization.
This consideration led, first, to the remarkable discovery ReUtiot
that several of the above primary forms are mere modifica- of faces
tions of each other, and ultimately showed that all crystals '" "°'-
found in nature may be referred to six systems, based on
certain relations of their axes, and that every face which
could occur upon a crystal bears a definite and simple
relation, in position and in angular incUnation, to these
axes.
As regards mere geometric measurement, there are several direc- Axes di-
tions in which axes may with nearly equal advantage be projected, rectioni
For example, in the cube
(fig. 19) tliey may bo drawn
from the centres of opposite
faces, as lettered O; or
from opposite solid Angles,
as lettered C ; or from the
centres of opposite edges,
as lettered D. There is
abundance of evidence that
each of those directions
must be regarded as lines
of dominant accretion of
molecules.
But the accretion may be
not only, dominant but
ovon\'helniingly so in one
only of these directions in
certain ciscs, or existent p,o J9_pp5iii„oof three sets of axes,
along one set of axes alone ;
in certain others. In a specimen of native silver from Alva in
Scotland (fig. 20), along 0 this is so much the case that the con-
creting molecules have done little more than delineate the form'
of an octahedron, and this they have only boeu able to do by
MINERALOGY
a4y
segregating tlemselves in lines of minnte crystals of the very
Btape of which they were projecting the skeleton form. More-
oTor, a polar aggregation at the terminal ends of these octahedral
dies is nere Jiown by the amount of concreting and crystallizing
Fig. 20.
material being larger at the terminations of these axes than else-
where. In the hollow-faced cube again (fig. 21), an aggregation
of molecnles in the direction of the lines D and C has tilled the
edges and solid angles while none have been deposited along 0.
Pig. 21. Pig. 2J.
This ocean in crystals tt nit. In t]l6 Iiollow-faced octahedron,
l^^ain (fig. 22), there has been no deposition of matter along the
line C. Cuprite often shows this form; and it as fi^«ently occurs
in hoUow-fai-ed dodecahedra, wherein tbe Tacuity is in the direc-
tion of D.
> In the specimen of pyrite from Elba (fig. 23), a deposition along
B and C would ultimately have erected the scaffolding of a hollow
cube, in twelve lines of minute
mmbinations of the cube and
Dctahedron. Such directional
arrangements may, moreover,
not only be iutermittent but
often alternate. The pyrite
from Traversella (fig. 24) is an
illustration of the first. A large
pentagonal dodecahedron hav-
ing been completed, a new ac-
cession of material has been
attached, iiot uniformly spread
over the pre-existent crystal,
to .enlarge it, but locally ar-
ranged, in equal amount, at
the poles of 6. But here the "°- ^•
special method of the arrangement has determined the formatien
of a number of small crystals of the same form as that originally
projected-
An altematioif, as it were, in plan is shown in such a crystal of
caldte as that in fig. 25. Here a scalenohedron is seen in the
centre of the figure ; then a rhombohedron has been perched »pon
its summit, tod iMtly both have been sheathed in a six-sided pnsm
witJa^hedtaLsununlti. .Different as tbw* 'bit* '•ims ao^jt is
found that they all here stand in a definite position one to the
other; that definite position is the relation which they bear to one
of tbe sets of axes, and this set may be assigned, not only to all
the three crystals here combined, but also to all the crjstals be-
longing to the same mineral, wherever occurring. This general
applicability constitutes one of the respects in which one special
set of axes is, in each of the systems, preferred to the othere.
I ' — ;
%]
1 / ;
u
Kg. 24. Fig. 25.
Another respect is the intensity with which the molecules cohere Coher-
in the different parts of the crystal, as refeiTed to these axes, and ence of
the resultant different hardness of certain parts of crystals. It particles
will be afterwards found that this obtains in a very limited notequal
manner in the crystals which belong to the first of the follow- j„ all di-
ing systems, on account of its regularity and sameness as a whole, recfions.
It may be laid down as a general rule that the edges of crystals are
harder than the centres of their faces, and the solid angles harder
than the edges. This is markedly the case in the diamond. But,
apart from this, there is no distinctive hardness in any one part, side,
or end of the crystals of the first system. It is otherwise with the
crystals which fall to be considered in all the other systems.
So different is the hardness of the various portions of these, so
diverse the appearance of their parts in lustre, colour, polish, ic.
so varying the amount of the recoil of these when struck, so unequal
their power of conducting heat, so dissimilar their power of re-
sisting the agencies of decay, and so irreconcilable their action upon
transmitted light, that we cannot but conclude that the molecules
which build them up are packed with greater force, if not in greater
number, in certain directions in preference to others. There thus
remains no question that these nature-indicated sets of axes are
those along which there has been a speciallv selective or " polar"
arrangement.
The six systema are foonded Upon the relationships of Systems of
the axes in nomber, in length, and in angular inclination, crystaji.
All crystals may be divided into " orthometric " or erect
forms and " clinometric " or inclined forms ; and in similar
manner may the systems be, through a consideration of
the relative lengths of their axes, divided into three classes.
In the first, or most regular, of these the axes are all equal,
that is, they are of one length ; in the second there is one
axis which differs in length from the others, and therefore
they are of two lengths; while in the third the axes are
all oneqaal, aad therefore they are of three lengths. Of
the six systems one belongs to the first class, two to the
second, and three to the third. Hence they are thus
classed : —
ilonomeiric
Cubic.
Dimetric.
Tetragonal.
HexagonaL
Triinetric.
Rieht Prisjnatic. ,
Oblique Prismatic
Anorthic.
Though the grouping of the systems into three classes
in virtue of axial diimensions is markedly bome out by
optical and other properties, yet it is altogether insufiScient
for determining the relationships of the myriad forms in
which bodies crystallize. Such knowledge is only attained
by combining the consideration of axial length, with axial
inclination ; and it is through a due regard of both oi these'
that the six systems are instituted.
The above table may be read in two different"wayB,—
either across or consecutively up and down the pagft
J The six av«tema ma."^ be tieated. of in either of these wain-
350
MINERALOGY
and there are certain advantages in considering them at
least first by the former method.
We consider first, as the more essential, the relative
lengths of the axes, and. secondly, the angular inclination
of these.
1. In the cubic system the axes are all equal, and all
intersect at right angles. Here is the most perfect sim-
plicity, and the most perfect regularity.
2. In the tetragonal system two only of the axes are
equal ; but all still intersect at right angles. Here ia a
departure from simplicity as regards the length of one axis,
but DO departure as regards the angular inclination.
3. In the right prismatic system none of the axes are
equal, but all still intersect at right angles. Here is total
loss of regularity in the first particular, but still none in
the second.
4. In the oblique prismatic system none of the axes are
equal, and only two intersect at right angles. Here there
is again a total loss of simpUcity in the first particular, and
a certain amount of departure from it in the second.
5. In the anorthic system none of the axes are equal,
and none of them intersect at right angles, — so that here,
as expressed by the name, there is
a total departure from regularity in
both particulars.
6. The hexagonal system is
anomalous in relation to this mode
of consideration. It is regarded as
having four axes, three of which lie
in one plane, parallel to the base, and
intersect each other at equal angles
Vnique
Fig. 27.
(necessarily angles of 60°).
The fourth axis intersects
these at right angles, and may
be longer, shorter, or equal
to them. This system is
generally considered after the
tetragonal system, as having
one axis which differs in
'length from the others, and
only one which cuts the
others at right angles. By
some a rhombohedron is con-
sidered as the primary of this
system ; it then comes to
have three axes, all equal,
but none intersecting at right
angles.
In considering these sys-
tems, or in describing the
form of a crystal, the vertical
or erect axis ia named the
principal axis of the figure,
and that axis is chosen as
the vertical which is the only
one of its kind. In the cubic
system there ia no such axis,
so that any one may be chosen as the vertical.
It will be convenient, before proceeding to the considera-
Stion of the laws of crystallograpliy and the combinations
Fig. 30.
of form.s, — especially in view of the terminology that must
be employed in illustrating those general aspects of the
subject, — to give an outline of one of the six systems here.
For this preliminary description the cubic system, as the
simplest and most regular, naturally suggests itself as the
most suitable.
I. The Cubic Sysian. — Here the axes are all equal, and Cubic
all intersect at right angles. The "cube" (fig. 26), "octa- syt^'"'
hedron" (fig. 30), and "rhombic dodecahedron" (fig.
33), which are here included, are ahke in their perfect
symmetry; the height, length, and breadth are equal;
and their axes are equal, and are rectangular in their
intersections.
In the cube (fig. 5) these axes connect the centres of
opposite faces; in the octahedron (fig. 15) the apices of
opposite soUd angles; in the dodecahedron (fig. 18) the
apices of opposite acute solid angles. The relation of these ReUtiou
forms to each other, and the correspondence in their axes, °' simple
wiU be made manifest through a consideration of the transi- "''""^
tion between the forms. If a cube be projected with the
axes in the above position, or if a model of it in any
sectile material be employed, and if the eight angles are
sliced off evenly, keeping the planes thus formed equally
inclined to the original faces, we first obtain the form in
fig. 27, then that in fig. 28 and fig. 29, and finally a
regular octahedron (fig. 30) ; and the last disappearing
point of each face of the cube is the apex of each solid
angle of the octahedron. Hence the axes of the former,
being in no way displaced, necessarily connect the apices
of the solid angles of the
latter. By cutting o£E as
evenly the twelve edges of
another cube, the knife being
equally inclined to the faces,
we have the form in fig. 31,
then fig. 32, and finally the
rhombic dodecahedron (fig.
33), with the exes of the cube
connecting the acute angles of
the new form. These forms
are thus mutually derivable.
Moreover, they are often pre-
sented by the same mineral
species, as is exemplified in
galena, pyrites, and the dia-
mond.
The process may be re-
versed, and the cube made
from the octahedron, as will
be readily understood from a
comparison, in reverse order,
of figs. 26 to 30. Or the cube
may be similarly derived from
the dodecahedron, as seen by
inspecting figs. 33, 32, 31, 26.
The octahedron also is
changed to a rhombic dodeca-
hedron by removing its twelve
edges (figs. 3-4, 35), and con-
tinuing the removal till the
original faces are obliterated,
thus producing the dodeca-
hedron.
It will bo observed that throughout aU these change*
the position of the axes, as determinant* of dimensions,
need not be altered, — that, in fact, one set of axes has
served for all the forms.
The relationships of the principal fonns of this system
being thus disclosed, the forms themselves have next to be
considered.
^^
Fig. 31.
MINERALOGY
Parts or . The cube (fig. 26) is bounded by six equal squares, has
tbaoube. twelve edges formed by faces meeting at 90°, and eight
solid trigonal angles. The axes are taken as joining the
centres of each two opposite faces. . Examples are hallite,
galena, and fluor.
Fig. 34.
Fig. 35.
.Dodeca-
hedron.
TetrakiS'
bexa-
hedrftQ.
MX/
0
^Sq^
\
jj2\,
0
Fig. 36.
Tritkis-
crtv
hedroD.
The octahedron (fig. 30), bounded by eight equilateral
triangles, has twelve equal edges with planes meeting at
109° 28' 16", and six tetragonal angles. The principal
axes join the opposite solid angles. Examples : magnetite,
gold, cuprite.
The rhombic dodecahedron, (fig. 33) is bounded by twelve
equal and similar rhombi, has twenty-four equal edges of
120°, and has six tetragonal and eight trigonal angles.
Each of the principal axes joins two opposite tetragonal
angles. Examples: garnet, cuprite, blende.
The tetrakishexahedrons (figs. 36, 37, 38, varieties of
icositetrahedron) are bounded by twenty-four isosceles
triangles, placed so as to form four-sided pyramids on the
faces of the cube, arranged in
six groups of four each. They
have twelve longer edges, which
correspond to those of the pri-
mitive or inscribed cube, and
twenty-fo'ir shorter edges placed
over each of its faces. The
angles are eight hexagonal and
six tetragonal, the latter joined
two and two by the principal
axes. Examples: fiuorite, gold.
This form varies much in general
aspect. The four-sided pyra-
mid which rests on the edges
of each face of the cube may be
so low as almost to fall into it
(fig. 36) ; or it may rise so high
that each side forms a level
surface with that which is ad-
jacent to it upon the nearest
cubic face (fig. 38). In the
latter case the form has become
the rhombic dodecahedron ; so
that the more or less acute
varieties of the form are but
stages of a passage of the cube
into the latter figure, through
an increasing accretion of matter
in the lines of the axes of the
cube. This is termed a " tran-
sition by increment."
The triakisoctahedrons, fig. 39
(variety of icositetrahedron,
fig. 40), are bounded by twenty-
four isosceles triangles, in eight
groups of three, ananged as pyramids on the edges of
the faces of the octahedron. Like the previons form
thsy vary in geneiml tspect, the variation here being from
Fig. 38.
351
the octahedron on one side to the rhombic dodecahedron
on the other ; while the increased accretion here is in the
direction of lines joining the centres of the faces of tha
octahedron or the solid angles of the cube. The passage
of the forms is similar to that illustrated in the last-coa-
Fig. 39.
Fig. 40.
•sidered form. The edges are twelve longer, corresponding
with those of the inscribed octahedron, and twenty-four
shorter, three and three over each of the faces. The angles
are eight trigonal and six ditetragonal (formed by eight
faces), the latter angles joined two and two by the principal
axes. Examples : galena, diamond.
The icositetrahedrons (fig. 40) are bounded by twenty- ic id-
four deltoids. This form varies from the octahedron to tetn-
the cube, sometimes approaching the former and sometimes h^l""-
the latter in general>aspect. A four-sided pyramid rests
on the angles of the faces of the cube. When increased
accretion takes place along the cubic axes, an octahedron.
results. When it is along lines joining the solid angles-
of the cube, that form itself results. The edges are twenty-
four longer and twenty-four shorter. The solid angles are
six tetragonal joined by the principal axes, eight trigonal,
and twelve rhombic or tetragonal with unequal angles.
Examples : analcime, garnet.
The hexakisoctahedrons (fig. 41), bounded by forty-eight Heztl^
scalene triangles, vary much in general aspect, approaching oet»- ^
more or less to all the preceding forms, into all of which "»o™*
they may pass ; but most frequently they have the faces
arranged either in six groups
of eight on the faces of the
cube,- or eight of six on the
faces of the octahedron, or
twelve of four on the faces of
the dodecahedron. There are
twenty-four long edges, often
corresponding to those of the
rhombic dodecahedron or bi-
secting the long diagonal of
the trapezohedron, twenty-four
intermediate edges lying in
pairs over each edge of the
inscribed octahedron, and twenty-four short edges in pairs
over the edges of the inscribed cube. There are six dite-
tragonal angles joined by the principal axes, eight hexa-
gonal, and twelve rhombic angles. Examoles : diamond,
fluorite.
General Laws of Crystallography. — The ^even forma of Laws oi
crystals noiv described are related to each other in the^^^J"*"
most intimate manner. This wiH appear more distinctly
from the account which is to follow of the mode of derivar-
tion of the forms, with which is conjoined an explana-
tion of the crystallographic signs or symbols by which
they are designated. These symbols were introduced by
Naumann, in the belief that they not only mark the forms
in a greatly abbreviated manner, but also exhibit th»
relations of the forms and combinations in a way which
words could hardly accomplish. In order to follow out this
r.g. 4L
T\IINERALOGY
Srinine-
Uy.
Parallel
iam of
faces.
Ratioii-
ility of
tlie iinv.1
metei"3.
60'^
derivation of forms, it is necessary to state briefly the
follo\. iig laws, whicli have been established in crystallo-
graphy. It is to be remembered that these laws apply,
not merely to the cubic system just described, but to all
the systems.
1. Tlie Law of tlie InrariahilUy of tlie Angles of Crystah,
' which was established by Romi de I'lsle, may be thus
stated : — the angles of inclination of the faces of a crystal
.Tre constant, however unequally the faces may be developed.
The corresponding angles of different crystalline specimens
of the same body do not, however, always absolutely agree.
Differences have been found, amounting sometimes even
to 10'.
2. The Law of Symmetry, discovered oy Haiiy, may
bo thus expressed: — (1) similar parts of crystals — faces,
edges, angles, and consequently axes — are all modified in
the same manner, and dissimilar parts are modified
sejiarately or differently; (2) the modifications produce the
same effect on the faces or edges which form the modified
jwrt, when they are equal ; when they are not equal, they
produce a different effect. That is, if an edge be truncated
or bevelled, eveiy simUar edge will be similarly truncated
or bevelled ; if an angle be truncated or acuminated, every
similar angle will be similarly truncated or acuminated ;
and consequently every similar axis will be equally affected
by the modifications. Thus the cube has eight similar
angles and twelve similar edges. In the physical produc-
tion of the cube, if one of the angles or edges be modified,
all will be sunilarly modified. This, which is the most
imjjortant law of crj'stallography, is, however, subject to
an exception which was fully foi;m\dated by Weiss. The
Jaw was — all the similar parts of crysfals, faces, edges,
angles, and consequently axes, are modified at the same
time and in the same manner; the forms resulting from
this law ai-s termed " holohedral." The exception is that
half of them or one-fourth of them only may be similarly
modified. ^\'Tieu only half of the similar parts are modi-
lied, we get the "liemihedral" forms; when one-fourth
only are modified, which occurs only rarely, we get
■' tefartohedral " forms.
3. The Law of the ParaUelism of the Facts of a Ciystal,
discovered by Romd de I'lsle, may be expressed as
follows : — every face of a crystal has a similar face parallel
to it : OP every, figiu-e is bounded by pairs of parallel faces
(with the exception of certain hemihedral forms).
4. I'lie Law of Zones, first established by Weiss, may be
thus enunciated : — the lines in which several faces of a
crystal intersect each other (or would do so if they were
produced until they met) frequently form a system of
]iarallcls. Such a series of faces is termed a "zone."
.sometimes the zones are parallel to one of the syi. metrical
axes. Thus, in every prism, the faces of the prism coii-
.stitute a zone which encircles the axis of the prism. Faces
may be in a zone although they do not actually intersect
on the form.
."). The Laic of the Pittionality of the Parameters of the
faces of crystalline series, first indicated by Malus, is that
the position of planes may bo assigned by numbers bearing
some simple ratio to the relative lengths of the axes of the
crystal. This law was the outcome of investigations into
the relationship of forms glanced at in commencing the
consideration of the cubic system, and was arrived at
thrqiigh the study of the mode of derivation of forms.
Tlic dcriviitiou of forms is tlint process I'y wliicli, from ono form
clioscn for tlio piunosi', .anvl consijtrcd os tlio type,— tlio fuoda.
,nii'ntiil or primaiy lorni,— all the other forms of a system may be
'|irojnceJ, acconliiig to fixed principles or general laws. In order
'o umlcratind this process or method of derivation, it must be noted
,hnt the position of any plane is fixed when the position of any
liree points in it, not all ni one straight line, is known. To deter-
-110 the position, therefore, of the lace of a crystal, it is only
necessary to know the distance of tlir^e points in it from the centre^
of the crystal, which is the point in which tlie a.tes intersect each
otluT. As the planes of all crystils are referred to their axes, the
points in ^vllich the face (or its supposed extension) meets the three
axes of the crystal are chosen, ana the portions of the axes twtween
these points and the centre are named parameters of tho face ; and Pan-
tile position of the faco is sulHciently known when tlie relative meten.,
lengtn or proportion of these paiantetcrs is ascertained. When the
jiosition 01 one. face of a sinijtle furni is thus fixed or described, all
the other faces of tlie form are in like manner fixed in accordance
with law 2, since tliey arc all equal and similar, and have equal
parameters — that is, intei-sect the axis in tlie sauio proportions.
Hence the expression which marks or describes one faco marks
and describes the whole figure, with all its faces.
The oetiiliedron is adopted as the primary or fundamental form
of the cubic system, and distinguished by the first letter of the
name, 0. Its faces cut the halr-.ixes at cpial distances from the
centre ; so that these semiaxcs, the p.uanictcr3 of tlie faces, have to
each other tlio proportion 1:1:1. In ordt-r to derive the other
forms from tlie octahedron, the following coiistiuction is employed.
Suppose a piano to be laid down jierpentlicular to one axis, and Propor
consequently [larallel to the two other axes (or to cut thcra at an in- tion of
finite distance, expressel by oo , the sign of infinity); then the para-
hexahedron or cube is produced, designated hy the crystallogiaphic meters
sign ooOoo, — expressing tlie proportion of the p.iranielcrs ol its express*
faces, or oo: 1 :oo. If a plane is supposed placed on each edge, by
parallel to one axis, and cutting tlie two other axes at equal dis- symbols.
tances, tho resulliiig figure is t^ic rliombic dodecahedron, designated Notatiou
by the sign o=0, tho proportion of the jiaranioters of its laces being of Nau-
a>: 1: I. The tliakisoctaliedrou arises when, on e.icli edge of the maiin.
"octahedron, planes are placed cutting the axis not belonging to that
edge at a distance frjm the centre vi, which is a rational number
greater than 1. Tne proportion of its paramctei*s is therefoiv
)ii ;1 : 1, and its sign mO ; tlie most common varieties are 50, 20,
and 30, seen in diamond and flnorite. When, oji the other hand,
from a similar distance vi in each two semiaxes prolonged a plane
is drawn to the other seniiaxis, or to each angle, an icositetrahedrou
is formed ; the parame.ers of its faces have consequently the pro-
portion m : 111 : 1, ami its sign is uiOi/i ; the most common varieties
are 202 and 303, — tho former Tciy frcqn?nt iu leucite, analcinic,
and garnet, the latter in gold and amalgam. When, again, planes
are drawn from each angle, «■ the end of Mie seniiaxis of tlie octa-
hedron, parallel to a second axis, and cutting tho third at a distance
11, greater than 1, then the tetraUislicxahedron is formed ; the para-
meter of its faces is oo : ii : 1 ; its sign is caOn ; and the most com-
mon varieties i» nature arc ooO|, od02, and oo03. Finally, if in
each seiniaxis of tho ocUhedron two distances w and ii bo taken,
each greater than 1, and m also greater than ii, and plniies bo dlawn
from each angle to these points, so that the two idan.a lying over
each edge cut the second soiuiaxis belonging to that edge at tho
smaller distance n, and tho third axis al tho greater distance »i,
tlien tho hexakisoctahedrou is piodueid; tho parameters are
HI : 11 : 1, its sign viOn, and the most common v.irielics 3&}, 402,
and 60J, seen iu diamond and Ihioritc.
It mnst bo observed that thc'nunibers in the above signs refer to
the par.imetcr^ of the fac«,— not to tlio axes of the crystal, which
are always equal. One parameter also h.as always been, in theabov*,
nssuiued -1, and Uicn, either one only of ihe two other ]iara-
nuters, marked by tho number before O, or boili of thc«i, niarkoj
by the nuinbera before and after O, liavo been chan^'ed.
In the above eousideratiou of the nioilo of dirivation of these
forms actually found in uatuie, which belong to the cubic nystcni,
it will be observed (though tho iHu«tiation3 w.re liniittd) that the
value of III and « in thesu indicated, by the preei^iuii ol' the inojior-
tioiis i!, 2, or 3, a definite nnnurieal rc-hitionsbip. This at once kj
up to the extended observations whieli established Iho law above
stated of proportionality in tho modification of crystals, or tlie
ratimiality of the parameters, which gives n matlienialieal bajis to
the science, adding to symnieliy of airaugeu'int a niiiiuiical rela-
tion iu tho position of the planes.
To illustrate tliis in n general form (ami not merely with special
reference to the mode of notation or expressi.ui of N.aiinianii, which
is that adopted in the subscpient descriptions), let AO.\', IJOU',
COC (Iig. 4-.!) be the three axes of a crystal, dniwii in pcre|nvtive,
and cnlting one another in the centre 0. Tlies.miaxis OA, OH, 00
are three p.-uaincter3. Now in the lino O.V take O.'.-IOA, niul
On.-JOA,— making as many j.oints as may be ll.■ce<i^ary be-
tween OA, rathnnlfmdioiisoi OA. Sul.dii ide OH and OV in a
similar manner. Fiu-ther produce 0.\, 01'., Of to Ao, D.>, Cu, in
each direction to an infinite distance, or to a sup|.us>-d inliuito
distance, as expressed by the arrow-head ; and suiqwe tlirse ex-
tended axes to bo divided iu a manner similar to the suKlivisioils
of tho parameters, bv rational multiples of OA, 01!, and OC. jlll
the plaws of a crystal will be parallel to om vr ollirr of tU plana
whichycjss through thru of the points thus dttrrmiiud.
First, in order to apjirehend the relationship of faces to these axes,
or to tho half axes,— the parameters of the faces,— let us bupposo ono
MINERALOGY
353
a
o»
3^»
0
^^bvJtJ^
■^
0
o3^
-'tl^ >
e >
*'
4-^
■"
plane of a crystal to bo so situated as to cut the three parameters
■OA, OB, OC at their extremities A, B, C, which it must De reraem-
Jxired are points equi-
distant from the centre ;
or let it be supposed
that a glass plate rests
u[ion three intersect-
ing wires at such
jioints. It is evident
that such' a plane or
plate will have a de-
Bnite y inclination or / ^,
shpe.! ' Suppose fur- "-rj-
ther "a second plane
or plate to exist,
which cuts the three
semiaxes in tke points
Oj,- Jj, Cj, which have
boen measured off
{along with a„ \, Cj)
as equidistant from O. -;
It will bo evident that •*
such a plane, though pj ^j.
smaller, will be parallel'
to tho first, seeing that, like it, it cnts the three parameters at
equal distances from 0.
A little consideration will show that, whatever the absolute dis-
tances from the centre may be, so long as the supporting subdivi-
sions are equal, no uew slope of the glass plates or planes is
possible ; planes so situated must be parallel and similar. Any sign
•which may be adopted to express the slope of one of such planes
must be applicable to all. A plane, however, cutting the points
Oj, 6i, C3 will have quite a different slope.
Let us now suppose a plane to cut a different set of the semiaxes,
namely, OA', OB', OC, in the points -Oj, -61, -c,. Such a piano
■would be parallel to one cutting the points - Oj, — ftj, - Cj, and also tp
the set of planes first described, but on the opposite side of the centre
of the crystal. If again, however, we had a plane cutting the semi-
axes OA' and OB' in - o^, - ftj, but the semiaxis OC iu the point
-C2, it is clear that the slope of this plane would be quite different
from thai of the planes Just described, but it would bo parallel to
the plane cutting the points Oj, dj, c^. This slope, like the other,
evidently depends, not on the absolute lengths of the portions of
OA', OB', OC cut off, bat upon their proportions or ratios; and
such is the case. with all the planes which are referred to the same
axes.
■ As there are three axes, and each or all of them may be cut at any
points and at any ratios, it is evident that the number of planes
which is possible is infinite ; and it must be also evident that tho
inclinations of all are fixed or determinate if we know the ratios.
AVhile, however, the possible number of planes is infinite, the actual
number occui-riug among minerals is either small or moderate, in
virtue of the fact that the ratios of subdivision of the axes are always
simple, and not numerous.
Other Naumann's symbols for the notation or individualizing of planes
nodea of have been glanced at. A simpler method is that of employing as
notatiui. indices the denominators (if simple fractions) of the fractional parts
of the axis cut. Thus ill is used for any plane parallel to that
cutting the axes in o,, \, Cj ; 122 for those parallel to Oj, i^, Cj ; 313
for a«, &i, C3 ; and so on.
When any of the points referred to have negative signs, the cor-
resi>onding indices have negative signs placed over_them. Thus
122 is the index for a plane parallel to c^-^^ 103 is the index
of the plane a',, Joo , d.. 00 nere indicates infinity ; that is, the
jdano never would cut the axis B however far it were extended ; in
other words, it is parallel to it. The necessity for elongating the
axes is broixght about by the occurrence of highly acuminating
pianos, which in many oases would not meet the axes at all unless
these were prolonged.
If the axes are unequal, as in the trimetric forms, then the ratio
is of the same character, except that the relative lengths of the axes
come into consideration ; but here, as in the regular system, irrational
values cannot occur, and iu even the roost complex crystals they
seldom exceed seven, either as aliquot parts or multiples.
It will thus be seen that in crystals there is no hapnazard scatter-
ing of faces, but a complete subserviency to law, a law which may
be said to be the linear equivalent to the law of multiple propor-
tions by weight, and Gay Lustac's law of multiple proportions in
combination by volume.
In abbreviation of all the systematic modes of notation, letters of
the Latin and Greek alphabets are frequently employed in a more or
less arbitrary manner, and with advantage in toe case of highly
complex forms.
2!'^'' 6. The Law of Symmetry of CrysUMine Combination
combiun. i^ ^^^ consequence of the law of symmetry and the law of
tiou. the rationality of the parameters, and has been partially
stated in enunciating these laws. It is thus expressed ; —
(1) a substance can only crystalline in forms, whethei-
simple or compound, which have the same relative
syihmetry, that is, belong to the same ' crystalline system,
and the parameters of the faces of which bear a simple
relation to each other, that is, belong to the same axis ; (2)
a form cannot be modified by "faces belonging to a different
system, or a different series.
. Certain exceptions to the first part of this law occur. Appai-ert
The element carbon occurs as the diamond, which is cubic, excep-
and as graphite, which is hexagonal. Sulphur occurs near '"""•
volcanoes in needle crystals belonging to the oblique
prismatic system, and also in caves (deposited apparently
from solution) in crystals belonging to the right prismatic
system. - Titanic acid is tetragonal in rutile, and right
prismatic in brookite. Carbonate of lime is hexagonal in
calcite, and prismatic in aragonite. These are probably
only apparent exceptions. The elementary substances
which go to form them occur in different allotropic states,
with different amounts of specific heat; and it is probable
that in these different states they go to form the above
modifications, which are therefore, iu every respect, except
in their chemical composition, different mineral bodies.
The physical differences between diamond and graphite
may suffice as an illustration. The diamond is trans-
parent, colourless, brittle, and extremely hard ; graphite
is opaque, black, tough, and so soft as to be utilized as
a lubricant.
Spheres of Projection. — The foregoing scheme for the
development of the relation which subsists bet>yeeu faces
of crystals and their axes affords but slight aid in display-
ing the position of the faces, or their mutual relationships.
The deliiieation even of a considerable series of crystal
forms does not indeed go far in effecting this, — on account,
first, of very unequal development in the size of the faces
of crystals, and, secondly, on account of the habit of
development of these faces not only differing largely, but
being special to certain localities,- — as in the entire absenee
of some faces, and in the preponderance of others.
Maps of the whole domain occupied by the forms of each Sphere*
mineral have been happily projected for such display. ?^P"'"
The projection is laid down as on 3 globe, in accordance J' °^
with stereographic projection, and admitting of calculation
according to the laws of spherical trigonometry. These
globe maps are called " spheres of projection." "The centre
O is the common centre of the crystal and of the sphere in
which the axes intersect. The three axes will of course
meet the circumference of the sphere in six points, called
the "poles of the axes." From the centre radii are
supposed to be drawn, meeting each plane perpendicularly.
It is evident that such radii will have fixed inclinations to
each other. They are called " normals " to the planes, and
the points in which when produced they meet the circum-
ference of the sphere of projection are called the " poles "
of the corresponding faces. A face and its pole thus call
for only one symbol The angle included by any two
normals is the supplement of that included by the two
corresponding faces.
It is thus easy to determine the angles of any two
normals when that of the corresponding faces is known, or
vice versa. Thus, if the angle between two faces is 125*,
that of the normals will be 5,5°. The spheres of projection
are specially adapted to enable us to avail ourselves of the
aid to calculation afforded by the forenoted fact that sets
of faces lie parallel to each other, forming zones ; for, when Zones,
projected on such a sphere, the normals of the parcel
faces will all lie in one plane ; and the poles, all cutting
its surface in the direction of one line, may be connected,
and so form a great circle on the sphere. This is called
the " zone circle. 'i_ A line drawn throueh the centre pf tti»
XYI. -- 45
354
MINERALOGY
zone plane, cutting it at right angles, Is the " zone a:ris " ; it
IS parallel to all the faces, and intersections of the faces (if
they are extended enough to intersect), of the zone. A face
may be common to two or more zones; its normals will then
coincide with the intersections of the several zone planes,
In the absence of actual spheres upon which to detail the
facts which go to form the "sphere of projection" o£ cacH
substance, the hemisphere is represented on a plane surface.
This has of necessity the disadvantage, except as regards
the circumferential zone, of introducing spherical distance-
distortion — foreshortening of all parts lying near the cir-
cumference ; but the eye soon gets accustomed to this. Fig.
43 presents the principal zones of the cubic system, and
Fib'. 43.
shows the position of the poles'* of the faces of the cube,
the octahedron, and the rhombic dodecahedron, o^, Oj, Or.
<kc., are the poles of the octahedral faces ; a^, Gj, a^, <fec., those
of the faces of the cube ; and d^^ d^ c?3, &c., those of Tue'
Vhombic dodecahedron. It will be observed that the faces
of the cube fall into the zone circles of the octahedron and
dodecahedron, while those of the octahedron fall into those
Frb. 44.— Principal Poles ot Cubic System in Octant of Sphere,
of the rhombic dodecahedron. Considering this as a
delineation of a globe, these zone circles come to re[)resent
latitude and longitude ; and, as almost all the faces in this
system fall into some zone circle, it is clear that the
latitude and longitude of all normals may be readily laid
dou*n, and their relations at .once determined by spherical
trigonometry. Fig. 44 shows the arrangement of tho poles
of all the forms belonging to the cubic system noticed
above, or referred *o in the present article, — delineated on
an octant of the sphere of projection. It displays the
perfect regularity of the system.
Hcmikedral and Tetartohcdral Forms.— The exception to the HemW
second law (that of symmetry), which was formulated by AVeits, hednJ
w;i3 to the effect that one-hall or even one-fourth only of the fnces forms.
which go to lormc. holohedrai crystal may be present. When but
one-half of the faces present thejnselves, the form is termed hemi*
hcJral; when ouly one-fourth, it'is tetartohcdral. These restrained
developments have now to be considered. In hcmihedral forms
the development is restrained, but symmetry is not deranged;
half the similar parts are still alike, though ruliku the otlior half.
There oie two classes of hemihedral fonns :
I. Those furms in whic> halt the similar angles or edges are
modified independently of the other half (*'hemi-holohedral"),
producing —
1. In the monoraetric and diraetric systems ' tetrahedral " and
"spheuoidal" forms, by the independeut replacement of the alter-
nate angles; tlieir opposite faces are not parallel, and they aro
hence called "inclined " hemihedrons; qs inchalcopyrite, boracite.*
The replacement in the dinietric system of two opposite basal edges
at one base and the other two at the opposite base is of the san*.
kind; as in ejingtonite.
2. In the trimetrin system *' monoclinic" forms, by the replace-
ment of half the similar parts of one base and the diagonally
opposite of the other, unlike the oth^r half; as in datholit<', humtte.
3. In the trimctric and hexagonal systems "hemimorphic "lorms,
by independent replacements at the opposite extremities of the
crystal ; as in topaz, calamine, tourmaline.
4. In the rhomboh^dral system, by the replacements of the
alternate basal edges or angles of the rhombohedron, forms usually
called **tet' ;x)hedral" or quarter forms, on the ground that
mathematically tho rhombohedron is a hemihedral form derived
from the hexagonal prism, which is the type of the hexngonul system.
Uock crystal is usually developed according to this Jaw.
II. Those forms in which all the siii,;lar angles or edges are
modified, but by half the full or normal number of planes {''holo-
hemihedral"), producing—
1. In the monometric system *'pyritohedral'* forms, by a replace,
nicnt of the edges or angles ; as in pyrites. Sucli forms have
opposite faces pai-allel, and are often called parallel hemihedrous.
2. In the dimetric system "pyramidar'aud "scalenoidal" forms,
by a replacement of the eight solid angles of the primary prism,
according to two raetthods.
3. In the hexagonal system " pyramoidal '' and "gTiToidal"
forms, by a replacement of the solid angles of the hexagonal
prism, or of the sis lateral angles of the rhombohedron, according to
two methods; as in quartz and apatite.
The above illustrations show that hemihedriem is not only
divided into two classes, but is of various kinds, and these have
been systematized as follows: — " holomorphic," in which tho
occurring planes pertain equally to the upper and lower (or opposite)
ranges of stct^ints, as in ordinary heraihedrons ; and (2) "lienii-
morphic,** in which each Get of planes pertains to cither the upi^or
or the lower range, but not to both. As to the relative position of
the sectants which contain the planes, the foims may be ^-cj'Iicallj
direct, as in baryte ; vertically alternate, as ia the tetrahedron, the
rhombohedron, and the plagilu-dral faces ot quartz ; and vtrtically
oblique, as in many forms of chonaroditc.
In hemimorphic forma symmetiy is deranged ; the crystals ai-e Demi-
bounded at t'le opposite ends of th:ii main axes by faces bdonging morphU
to distinct formi. or modifications. — always,
however, of the same system ; hence only tJie
upper or tlie \iuder half of each ciystal can be
regarded as complete, as i-egards tlitform there
seen ; and so for each end it is half formed.
Fig. 45 i-cprescnts a crystal of tourmaline,
which is bounded
on the upper end
by the planes of
the rhombohedrons
Ji{P) and -2R{o),
and on the lower
end by the basal
pinncoid (f)- In
tig. 46 of smith-
sooito tho u}iper
oxtromity shows the
banc k, two brachydomes o oiul ;), and two macrodomes
' As the parts of either half arc .iltcniatc, there still results a fynime-
tiicil solid. At> either one or other half may be the one thus modified,
there may result two such symmetric solid% which stand in an invrrid
]TOsition to one another. When the moditlcatioas affect the upper right-
hand solid nnj;lc, the resulting torra is calle'* + ; when the upper Iffl-
haud angle it is-.
\ ftnd /;
MINERALOGY
355
whilst on the lower end it is bounde J by the faces P of the primary
tlone.
It has been found that all hemimorphic crystals become electri-
cally polar when heated, that is, exhibit opposite kinds of electricity
at opposite ends of the crystal. The subject will he more fully con-
sidered under the electricity of minerals.
The hemihedral forms of the cubic system are the following : —
1. The tetrahedron (fig. 47), hemihedral of the octahedron, is
bounded by four equilateral triangles. It has six equal edges with
faces meeting at 70° 32', and four trigonal angles. The principal
axes join the middle points of each two opposite edges. Examples :
^ahlore, boracite and helrine.
Fig. iS.
2. The trigonal dodecahedrons (fig. 48), hemihedral of the icosi-
tetrahedron, are bounded by twelve isosceles triangles, and vary in
general form from the tetrahedron to the cube. There are six longer
edges corresponding to those of the inscribed tetrahedron, and
twelve shorter, placed three and three over each of its faces, and
fonr hexagonal and four trigonal angles. Example : tetrahedrite.
3. The deltoid dodecahedrons (fig. 49), hemihedral of the triakis-
octahedron, are bounded by twelve deltoids, and vary in general
form from the tetrahedron on the one hand to tlie rhombic
dodecahedron on the other. They have twelve longer edges lying
in pairs over the edges of the inscribed tetrahedron, and twelve
shorter edges, three and three over each of its faces. There
are six tetragonal (rhombic), four acute trigonal, and four obtuse
trigonal angles. The principal axes join, two and two, opposite
thombic angles. Example : tetrahedrite.
.Fig. 49. Fig. 50.
4. Tlio hexakistetrahedrons (fig. 60), hemihedral of the hexakfs-
octahedron, are bounded by twenty-four scaler.e triangles, and most
commonly have their faces grouped in four systems of six c-xch.
'i'he edges are twelve shorter and twelve longer, lying in groups of
three over each face of the inscribed tetrahedron, and twelve in-
termediate in pairs over its edges. The angles are six rhombic,
joined in pairs by the principal axes, and four acuter and four
obtuser hexagonal angles. Exanple : diamonu.
In these forms, often named " tetr . jedral," the faces are oblique
to each other. TTieir derivation and signs are as follows. The tetra-
hedron arises when four alternate faces of the octahedron, two
opposite above and two intermediate below, are enlarged so as to
obliterate the other fcnr ; and its sign is hence — . Bu';, as either
four faces may be thus enlarged or obliterated, two tetrahedrons can
be formed, sirafiar in all respects except in position, and together
making up the octahedron. These are distinguished by the signs +
and - , added to the above symbol, but only the latter in general
expressed, thus •
, In all hemihedric systems two forms simi-
ttrly related occur, which may thus bo named complementary
forms. The trigonal dodecahedron is derived from the icositetra-
bedron by the expansion of the alternate trigonal groups of faces.
,. . . mOm ., ,^ ■ . I • 202 / __
Its- sign IS —I , the most common vanety berng —^ . dne
deltoid dodecahedron is in like manner the residt of the incresise of
the alternate trigonal groups of faces of the triakisoctahedron, and
tts sign is
mO
Lastly, the hexalcistetrahedron arises in the
development of alternate hexagonal groups of faces in the heza^
kiaoctahedroD, and its sign is — -—
Two semitesseral forms with parallel faces occur. (1) The
pentagonal dodecahedrons (fig. 61), bounded by twelve symmetrical
pentagons, vary in general aspect between the cube and the rhombic
dodecahedron. They have six regular. (and in general longer)
edges, lying over the faces of the inscvibsd cube, and twenty-
Fig. 51.
Fig. 52.
four, generally shorter \seldom longer), edges, usually lying in
pairs over its edges. The solid angles are eight of three equal
interfacial angles, and twelve of three interfacial angles, of \?iiich
only two are equal. Each principal axis unites two opposite regular
edges. This form is derived from the tetrakishexahedron, and its
sign is — - — . It is found frequently in iron pyrites and cohaltine.
(2) The dyakisdodecahedron (fig. 52), bounded by twenty-four
trapezoids with two sides equal, has twelve short, twelve long, and
twenty-four intermediate edges. The angles are six equiangular
rhombic, united in pairs by the principal axes, eight trigonal, and
twenty-four irregular tetragonal angles. It is derived from the
hexakisoctahedron, and its sign is I 1 , the brackets being
used to distinguish it from the hexakistetrahedron, also derived
from the same primary form. It occurs in iron pyrites and
cobaltinc. The two other semitesseral forms, the pentagonal
Fig. 63. Fig. 54
dodecahedron (fig. 63), and the pentagonal icositetrahedron (fijj
54), both bounded by irregular pentagons, have not yet ,been
observed in nature.
CombiruUions. — The above-mentioned forms of the tes- Comhin*
serai system (and this is true also of the five other systems tions. -^
of crystallization) not only occur singly, but often two,
three, or more occur united in the same crystal, forming
■what are named combinations.
In this case it is evident that no one of the individual
forms can be complete, because the faces of one form mu.st
interfere -with, by diminishing, the faces of other forms.
A combination therefore implies that the faces of one form
shall appear symmetrically disposed between the faces of
other forms, and consequently take the place of certain
of their edges and angles. These edges and angles are
thus, as it were, cut off, and a greater number of new
ones produced in their place, which properly belong neither
to the one form nor the other, but are angles of combina-
tion. These new faces are hence termed modifications,
and the original or primary or simple form is said to be
modified. Usually one form predominates more than the
ethers, or has more influence on the general aspect of the
crystal, and hence is distinguished as the predominant
form, the others being considered subordinate.
The sign of the combinstion consists of those of its constitnenl
forms, written in the order of their influence or importance in the
combination, with a point between each pair.
ItwiU be readily seen that such combinations may be exceedingly
nnmerouB, ar rather infinite ; and only n. *>w of the more common
356
MINERALOGY
can be noticed. Many others raoro complicated will occur in the
descriptive pnrt of tliia article. Among bolohodral combinations,
tlie cube, octnhoilron, and rhombic dodecahedron are the predomin-
ant forms. In fig. 27 the cube has its angles replaced by the faeoa
of the octahedron, which truncate the angles, and the sign of this
combination is coOoo , 0. In fig. 28 this process may be regarded as
having proceeded still farther, so that the faces of the octahedron
nearly equal those of the cube, while in fig. 29 they now predom-
inate ; tne sign, still of the same two elements, but in reverse
order, is 0, ooOoo . It will thus be seen that, through an increase in
the amount of the abstraction of the faces of the cube, the figure
gradually passes over into that of the octahedron. This may occur
in all cases, and is termed the passage of the cube into the octa-
hedron (or vice versa), or a " transition by decrement."
In fig. 31 the cube has its edges replaced by the faces of the
rhombic dodecahedron, which truncate the eJges, the sign being
ooO=o,ooO; while m fig. 32 there is the same combination, but with
the faces of the cube subordinate, and hence the sign is ooO, ooOoo.
The former figure, it will be seen, has more the general aspect of the
cube, the latter of the dodecahedron. Here the solid angles of the
latter are truncated by the faces of the cube, and we have the
passage of the cube into the dodecaliedron by decrement. The
same transition, through truncation or decrement, could be shown
in all cases of combinations, and in both directions, the last stage
of the passage into one or other form always consisting of the
replacement of its solid or interfacial angles by facee of the de-
parting figure, more or less minute. A few illustrations of this
may be given, in the three most important forms.
The relationship of the tetrakishexahcdron to the cube has
above been stated to be, that its faces form si.x low quadrilateral
pyramids, which rest upon or spring from the edges of the cube.
(From this the form derives its trivial name of four-faced cube.)
Hence these faces bevel the edges of the cube. The first stage of
such bevelling (or the last stage of the truncation of the tetmkis-
hoxahedrou by the faces of the cube — whichever way it may be
regarded) is seen in fig. 65. As the cubic face is here dominant,
the sign is ooOco , oo03. Fig. 56 shows a somewhat similar stage
^<f \^J^
y-'i ■■ 1
y
spH
; i
1 i
..•1. 1 ,-•'
s
z
i
I
Fig. 55.
Fig. 66.
in the modification produced through the combination of the icosi-
tetrahedron with the cube. The trilateral pyramid which this
form places upon the faces of the cube rests upon its solid angles,
instead of, as in the last case, upon its edges ; hence it is these
solid angles which, in the process of decreuient, it replaces by faces
which form a low three-sided pyramid. The triakisoctahedron,
Fig. 67.
Fig. 58.
again, modifies the solid angles of the cube, as shown in fig. 57, by
& low three-sided pyramid, positioned at right angles to that
considered in the last combination. As
the hexakisoctahedron is merely the
two-faced form of that last considered,
the pyramid which modifies the solid
anglos is, in its combination with the
cube, six-sided, as in fig. 58.
As the faces of the rhombic dodeca-
hedron truncate the edges of the octa-
hedron, fig. 34 represents the first stngo
of such truncation or combination; while
fig. 35 may be taken as representing the
last, the faces of the octahedron being
there nearly totally removed.
Fig. 69 shows the first stage of the
passage of the octahedron into the icosi tetrahedron, in the trunca-
" tioa of the solid angles of the fornjer form by a foui"-sided pyra-
Fig. 69.
mid formed by the (6 x 4) faces of the latter. The facc8 of the
octahedron truncate the three-faced solid angles of the rhombic
dodecahedron. Fig. 35 shows the first stage of thia truDcation,
while fig. 34 shows an advanced amount. The faces of the icosi-
Fig. 60. Fig. 61.
tetrahedron truncate the edges of the rhombic dodecahedron, as in
fig. 60 ; while those of the latter truncate the unequal- angled tetra-
gonal (or rhombic) angles of the former (fig. 61). The faces of the
hexakisoctahedron bevel the edges of the rhombic dodecahedron.
While such transitions may appear indefinite, yet certain
minerals have either in themselves a habit, or have at certain
localities a habit, of crystallizing so markedly in a certain stage
of these transitions as to be absolutely capable of recognition
thereby.
Combinations of hemihedral or, as they have been called, bcmi- Combina-
tesseral forms are of three classes: — those with holohedral forms, tions of
those in which the faces fall obliquely on one another, and those hemi-
with parallel faces. Fig. 62 shows the combination of a right- bedral
forms.
Fig. 62.' Fig. 63.
hanoed tetrahedron with the cube, which truncates its edges, the
tetrahedron here being dominant. Fig. 63, again, shows a 0(Jm-
bination of the cubo-dodecahedron with a right-handed tetrahedron,
the first or holohedral form being in this case markedly dominant.
Fig. 64 is an illustration of the second class, combinations of
Fig. 64. Fig. 65.
obliauc-faced semitcsseral forms with each other. In it s right-
hauaed tetrahedron has its solid angles truncated by the facr« of
one which is left-handed ; and so its sign is — , . Fig. 66
shows a combination of a right-handed tetrahedron with a left-
Fig. 66. Fig. 67.
handed three-faced tetrahedron. Fip. 66 shows a combinotibn of
a right-han<lod hemihcdron of the icositetrabc<Iron with a right-
handed tetrahedron.
Parallel-faced homihedrons generally form combinations with
hololiodral forms ; and the amount of relati^•c dorunanco is of oil
degrees. Fig. 67 shove a combination, in equal amount, of the cubff
MINERALOGY
357
■JRtli » Tflrtic&^.facea pentagonal dodecahedron; while fig. 68 shows
an increase in the amoont of trancation effected bj the latter. Fig.
§9 shows the combination of the cube with the djakidodecohedron.
Fig. 68.
Fig. 69.
the former being dominant. In fig. 70 an octahedron, in dominance,
is combined with the vertical-faced pentagonal dodecahedron; in
Fig. 70. Fig. 71.
fig. 71 the faces of these forms are of nearly equal size, while in
fig. 72 the octahedral faces are nearly remoTed. The solid angles of
Fig. 72. Fig. 73.
tbe octahedron are modified in Sg. 73 by the foces of the dyalds-
dodecahedron. In fig. 68 a vertical'iaced pentagonal dodeca*
Fig-_74. Fig. 75.
hedron is the prevailing form in combination with the cabe; while
in fig. 74 the faces of the octahedron are superadded. In fig. 75 its
octahedral angles are modified by the faces of the icositetrahedron,
Fig. 76. Fig. 77.
and in fig. 76 by those of the Oo^hedron in addition. In fig.
77 they are modified by the faces of the dyakisdodecaliedron.
In etkch of the five systems which follow there is this
difference from the cubic system that one axis is always
tmequal to (longer or shorter than) the others. This is
placed erect, and named the chief axis ; its ends are poles, Dimetrie
and the edges connected with them polar edges. The ""d
other axes are named subordinate or lateral axes, and the '"metric
plane that passes through them is the base. A plane "'""''
through the chief and a lateral axis is a normal chief
sectioru In these systems also occur the three forms of
"pyramids," "prisms," and "pinacoids." (1) The pyra-
mids have their faces triangles. Pyramids in crystallo-
graphy are each composed of two geometric pyramids
placed base to base, and named "closed forma," as the
crystab are shut in by definite faces on every side. (2)
The prisms are bounded by plane faces parallel to one axis.
They are thus of unlimited extent in the direction of that
axis, and therefore named "open forms," but in solid crystals
are. shut in by feces of other forms. (3) The pinacoids, or
tables, have two faces intersecting one axis and parallel
to the others, and thus are also open forms, or unlimited iu
the direction of these axes. Forms (2) and (3), when con-
joined, mutually shut in each other, or produce closed forms.
IL Pyramidal or Tetragonal System. — This system has Pyra-
three axes at right angles, two of them equal, and the chief """^^l
axis longer or shorter. The name tetragonal is derived ^^''^"^
from the form of the base, which is usually quadrangular.
There are eight tetragonal forms, of which five are closed. (1)
Tetragonal pyramids (figs. ?8, 79) are enclosed by eight isosceles
triangles, with four middle edges all
in one plane, and eight polar edges.
There are three kinds of this form,
Fig. 79.
Fig. 78.
distinguished by the position of the
lateral axes. In the first these axes
unite the opposite angles ; in the second
they intersect the middle edges eaaally ; and in the third they
lie in an intermediate position, or divide these edges unequally, —
the la*t being hemihcoral forms. These pyramidsjare also dis-
tinguished as obtuse (fig. 78) or acute (fig. 79), according as the
vortical angle is greater or less than in t^e
regular octahedron. (2) Ditetragonal pyra-
Tnids (fig. 80) are bounded by sixteen scalene
triangles, whose base-lines are all In one
Fig. 80, Fig. 81.
plane. This form rarely occnrs except in combinations. (3) Tetra-
gonal sphenoids (fig. 81), bounded by four isosceles triangles, are
the h^mihedral forms of the first variety of tetragonal pyramids.
H) The tetragonal scalenohedron (fig. 82), bounded by eight scalene
triangles, whose bases rise and fall in a ziraig line, is tlie hemi-
hedral form of the ditetragonal pyramid. Nos. (3) and (4) are rare.
(5) The tetragonal trapezohedron is not found in minerals as a simple
form. The three open forms are — (1) tetragonal prisms, bounded
by four planes parallel to the principal axis, which may be either
longer (fig. 83) or shorter (fig. 84) than the lateral axes; (2) dite-
tragonal prisms, bounded by eight similar planes; and (3) the basal
pinacoid, consisting merelv of two parallel faceslMuuding the pnsms
at the ends, above and below. • . > »
Tli« various series of tetragonal crystals are distinguished from
each other only by their rthitive dimensions. To determiae these.
3r)8
MINERALOGY
Prinii- one of the series most be chosen as the primary fonn, and for this
live purpose a tetragonal pyramid of the first variety, designated by P
pyramid, as its sign, is selected. The angle of one of its edges, especially
the middle edge, found by measurement, determines its angular
dimensions, whilst the proportion of the princiual axis a to the
Deii
Fig. 82, Fig. 84.
lateral axes, supposed equal to 1, giTes its linear dimensions. The
parameters, therefore, of each face of the fundamental form are
1 : 1 : a.
Now if m be any (rational) number, either less or greater than
unity, and if from any distance ma in the principal axis planes be
drawn to the middle edge of P, then new tetragonal pyramids of
the first order, but more or less acute br obtuse than P, are formed.
u\ The general sign of these pyramids is mP, and the most common
varieties JP, 2P, and
-with the chief
axis half, twice, or
thrice that of P. If
m becomes infinite,
then the pyramid
Prism. passes into a prism,
indefinitely extended
along the principal
axis, and with the
sign ooP. If 7n«0,
which is the case
when the lateral axea
are supposed iufinite,
then it becomes a
Pinacuid. pinacoid, consisting
f)roperly of two basal
aces open towards
the lateral axes, and
designated by the
sign OP. The ditetra-
gonal pyramids are
produced by taking
in each lateral axis
distances n greater
than 1, and drawing
Vvo pianos to these
points from each
of the intermediate
Fig. 86.
Fig. 87.-
polar edges. The parameters of these planes are therefore m : 1 : n,
and the general sign of the form mPti, the most common values
of 71 being ^, 2, 3, and oo. When 7i — co, a tetragonal pyramid of
the second order arises, designated generally by jnPoo, the most
common in the mineril kingdom being Poo and 2Poo . The relation
of these to pyramids of the first order is sliown in fig. 85, where
ABBBC is the first and ACCCX the second order of pyramid. In
like manner, from the prism oop, the ditetragonal prisms ooPn
Fig. 88. Fig. 89.
aw derived, and, finally, when n-oo the tetragonal prism of the
•econd order, whose sign ia ooPoo.
The couibiuatiottfl ofthc tetragonal sysUm are either holohcdral
or liemihedral ; but the latter are rare. Prisms and pinacoida
must always be terminated on the open sides by other forms. Thus
in fig. 86 a square prism of the first order is terminated by the
primary pyramid, and has its lateral angles again replaced by
another more acute pyramid of the second order, bo that its sigQ
is wP, P, 2Pc
In fig. 87 a prism of the second order ia first bounded by the
fundamental pyramid, and then has its 'edges of combination
replaced by a ditetragonal pyramid ; its sign is odPoo, P, 3P3. In
fig. 88 the polar edges ol the pyramid are replaced bv another
pyramid, its sign being P, Pco . In fig. 89 a hemihedric form, very
characteristic of chalcopyrite, is represented, — P and F" being the
two sphenoids, a the basal pinacoid, and b, c two ditetragonal
pyramids.
m. Tlie Hexagonal System. — The esserftial character of B«h&
this system is that it has four axes, — three eqnal lateral 8<»^
axes intersecting each other in one plane at 60", and one ''***™'
principal axis at right angles to these. The plane through
the lateral axes, or the base, from its hexagonal form, gives
the name to the system. As in the last system, its forms
are either closed or open. They are divided into holohedral,
hemihedral, and tetartohedral, — the last, which are rare,
having only a fourth part of the faces developed. Only a
few of the more common forms require to be here described.
The hexagonal pyramids (figs. 90, 91) are bounded by twelve P>il»-
isosceles triangles, and are of three kinds, according as the lateral nud»
axes fall in the angles, in the middle
of the lateral edges, or in another
point of these edges, the last being
hemihedral forms. They are also
classed as acute or obtuse, but with-
out any precise limits. The trigonal
pyramid is bounded by six triangles,
and may be viewed as the hemihedral
form of the hexagonal. The dihexa-
gonal pyramid is oounded bv twenty-
four scalene triangles, but has never
been observed alone, and rarely even
in combinations. The more common
prisms are the hexagonal of six sides ;
in these the vertical axis may be
either longer than the lateral, as in
fig. 92, or shorter, as in fig. 93.
There are also dihexagonal, of twelve
sides,
A-particular pyramid P is chosen
as the fundamental form of this
system, and its dimensions deter-
mined either from the proportion of
the lateral lo the principal axis (1 : a) ,
or from the measurement of its angles.
From this form (mP) others are de-
rived exactly as in the tetragonal
system. Thus dihexagonal pyramids
are produced with the general sign
mPri, the chief peculiarity being that, ^^^- ^*-
whereas in the tetragonal system n might have any rational value
from i to 05, in the hexagonal system it can only vary from 1 to
2, in consequence of the geometric character "of the figure. When
n-2, the dihexagonal changes into an hexagonal pyramid of the
second order, whose sign is MiP2. When in — oo. various prisma
arise from similar
the
changes ir
of 71 ; and wheniJi-O
the basal pinacoid is
formed.
Few hexagonal min-
eral sncriea form per-
fect holohcdral com-
binations. Though
quartz and apatite ap-
pear as such, yet pro-
perly the former is a
tetartohc<lral, the lat-
ter ft hemihedral spe-
cies. In holohedral
species the predomi-
nant fAces are usually
those of tho hexiigonal Fig. 93. Fig. 94.
prisms ooP (fig. 92) and ooP2, or of the pinacoid OP (fig. 93); whilrt iTifcOii,
the pyramids t* and 2P2 aro tho moat common subordinate forms.
Fig. 94 represents tho prism, bounded on the extremities by two
p)ramidS|— ouC| P, forming ihp apex, the other, 2P2, the rhombic
MINEEALOaY
359
face* on tBe angles, or «x>P, P, 2P2. Fig. 95 ia a sinrilar form, the
upper part of the pyramid being replaced by the pinacoid. In
some crystals the lateral edges of the prism are replaced by the
KxV
Fig. 95. Fig. 96. Fig. 97.
second prism osP2 (fig. 96), producing an ejuiangnlar twelve-sided
prism, which always represents the combination ooP, odP2, and
«aimot occur as a simple form. Figs. 97, 98 are combinationa iu this
Fig. 88. Fig. 99.
system seen in beryl. An example of a more complicated combina-
tion is seen in fig. 99, of a crystal of apatite, whose sign with the
corresponding l-?tterais o<,P(J/), cxP2(«), OP(i'), }P(r), P(x), 2PCz),
P2(a), 2P2(s), 4P2(d).
Hexagonal minerals frequently crystallize in those series of hemi-
hedral forms that are named " rhoinbohedral," from the prevalence
in them of rhombohedrona. These (figs. 100. 101) are bounded by
Fig. 100. Fig. 101.
six rhombi, whose lateral edges do not lie In one plane, bnt rise and
fall iu a zigzag mauner. The principal axis unites the two trigonal
angles, formed by three e<jnal plane anglea ; and in the most
variety the secondary axes join the y^-
middle points of two opposite edgea.
"When the polar edges form an angle of
tnore than 90°, the rhombohedrons are
oamed obtuse ; when of less than 90°,
acute ; fig. 102 represents the first, fig.
103 the second. Hexagonal scaleno-
bedrona (fig. 104) are bounded by
twelve scalene triangles, whose lateral
Fig. 102. Fig. 103.
edges do not lie in oco plane. The principal axis joins the two
hexagonal angles, and the secondary axis the middle [winta of two
opposite lateral edges.
The rhombohedron is derived from the first order of hexagonal
pyramid by the hemih6di*al development of its alternate faces. Its
general sign should therefore be . — . ; but on several grounds it ia
jbuud better to designate it by R or tnP, and its complementary
figure by-mR. Wlien the prism or pinacoid arises as its limiting
form, they arc designated by ooR and OR, though in no respect
changed from the limiting forms fsP and OP o{ the pyramid. The
scalenohedron is properly the hemibedral form of the dihexagonal
pyramid, bnt ia more easUy understood as derived from the inscribed
rhombohedron mR. If the halves of the principal axis of tUgj
be multiplied by a- definite number
n, and then planes be drawn from
the extremities of this enlarged axis
to the lateral edges of the rnombo-
licdron, as in fig. 105, the scaleno-
hedron is constnicted. It is now
designated by mRji (the n on the
right here referring to the chief axis),
and the dihexagonal prism in this
series by oo Rn (for-
merly TnR" and
coR").
The combina-
tions of rhombo-
hedral forms are
very numerous,
several hundreds
having been de-
scribed in calc-spap
alone. Among tha
most common ia
the prism in com-
bination with a
rhombohedron, aa
seen in the twin
crystal of calc-
spar (fig. 106),
with the
ooR, - JR, the lower half being the same form with the upper, but
turned round 180°. In fig. 107 the rhombohedron mRbaa its polar
Fig. 1051
Fig. 106. Fig. 107.
edgea replaced by another rhombohedron - JmR, and in fig. 108
its lateral edges bevelled by the scalencihearon mRn. A mora
complex combination of five forms
is represented in the ciystal of calc-
spar fig. 109, its sign, with the
letters on the faces, Deing R''(i/),
Fig. 108. Fig. 109.
R'()-\ R(P), 4R(.m), ooR(c,. Tetartohcdral combinationa are aeea
moat distinctly in rock-crystal.
rV. Right Prismatic or Rhombic System. — This syetem Rigiit
13 characterized by three unequal axes, all at right angles prismaUe
to each other. Any one of these may be assumed aa the system,
chief axis, when the others are named subordinate. Tho
plane passing through the secondary axes, or the base, forms
a rhombus, and from this one of its names is derived. Aa
priftmatic forms are most frequent (the prism standing
vertically on the rhombic base), it is best defined as tha
right prismatic. This .system comprises only a few varie-
ties of forms that are essentially distinct, and its relations
are consequently very simple,
360
Ml^'ERALOG'i:
pyra- There tire two closed forms. (1) The rhombic pyfamldsCfigs. 110,
mills. Ill), bounded by eight scalene triangles, whose lateral ijclges lie inone
Fig. 112.
Fig. lU.
Fig. 110.
plane, and form a rhom-
ous. They have eight
polar edges (four acute
and four more obtuse'
nnd four lateral edges.
The angles are six rhom-
bic, the m63t acute at
the extremities of the
longest axis. (2) The
rhombic sphenoids (figs. 112, 113) are bounded by four scalene
triangles, with their lateral edges not in one plane, and are hemi-
hedrai forms of the rhombic pyramid.
They are of very infrequent occurrence.
The open forms, agai n, are rhombic prisms
bounded by four planes parallel to one
of the axes, which is indefinitely ex-
tended, and may be longer than the
lateral, as in fig. 114, or shorter as in
fig. 115, Thoy are divided into uj^right
(as in the above figs.) and horizontal
prisms, according as either the principal
or one or other of the lateral axes is
supposed to become infinite. For the
latter form the name doma or dome has
been used ; and two kinds, the macro-
dome (fig. 116) and the brachydome (fig.
117), have been distinguished.
Pinacoida. Rhombic pinacoids also arise when
one axis becomes =Oand the two others
Kphen-
Pvisms,
Fig. 113.
! I
Domes.
Fig. 115.
indefinitely extended ; and so we
have macropinacoids (fig. 118) and
brachy pinacoids (fig. 119), — the qualifying term thus designat-
ing tno axis 'to wliich the faces of the dome or pinacoid are
parallel.
In deriving these forms from a primary, a particular rVombic pyra-
mid P is chosen, and its dimensions determined either from the
bracl^y-
djagunal.
•"•6 —"■"'_-
rodiagonal is
Fig. 116. Fig. 117.
angular measurement of two of its edges, or by the linear pro-
portion of its axes a: b: c, the greater lateral axis b being assumed
Oiiuai to 1. To the greater lateral axis the name
givfu, to tlie shorter that of
Lrochydiagonal ; and the two
princii>al sections are in like
joanuor named macrodiagonal and
hr-K-hyliogonnl, according to the
axis they intersect. The some
terniM are applied throughoiU all
the derived torina. They conse-
quontly mark only the position of
tno faces in rt-sjwct to the axes fjg_ np
of the fundamental crystal ""''
Pig. 119.
of tho fundamental crystal and ' , , . ...
frenuontly of necessity l^-iC^ott reference to tho relative magnitude
of tno derived axes. A ■ i u
By multiplying tho principal axis by any rational nnmbrr m,
greater or ioss than 1, a scries of pyramids arise, whose general sign Deri
Ls mP, and their limits are the prism and pinacoid ; the whole senes fonffr
befng contained in this formula, OP ... . 7nP . . . . P . . .
mP .... ooP, — which is the fundamental series, tho lateral axes
always remaining unchanged.
From each member a new series may, however, be developed in
two directions, by increasing one or other of the latend axes, when
the macrodiagonal is
thus multiplied by any
number n greater than
1 , and planes drawn
from the distance n to
the polar edges, a new
pyramid is produced,
named a macropyramid,
with the sign m^n, the
mark over the P point-
ing out the axis en-
larged. When jt — CO,
a macrodome results,
with the sign wiPoo.
If the shorter axis is
muVtiplied, then brachy-
pyramids and brachy-
domes are produced^
with the signs mr7i and
TJif oo . So also from the
prism coP, on the one
side, originate numerous
macroprisms oopjt, yitb
the limiting macro-
piiiacoid ocpoo ; on the
other, numerous brachy
prisms ooPn, with the
limit form oofco, or the brachypinacoid. In figs. 120, 121 the
two domes are shown in their relation to the primitive pyramid
Fig. 121.
Fig. 123.
Fi«. 124.
The pyramids seldom occur independent, or even as the pre-
dominant forma in a combination; sulphur, however, ia an ezcop*
tion. Prisms or pinacoids
usuallygive the general char-
actor to tho crystal, which
thou appears cither in a
columnar or tabular or even
rectangular pyramidal form.
Tho ' determination of the
position of these crystals, as
vertical or horizontal, de-
pends on tho choice of the
chief axis of the fundamental
form. In the toj^az crystal
(6g. 12*2) tho brachypribm
and tho pyramid are tlic
predoroinnnt elements, asso-
ciated with the prism, it-*,
sign and letters being
(xl»2(0. P(o). «P(irt. Fig.
123 of Blilbito is another
example, the macropin'acoid
00 poo or J/ being combinM
.ith th. pyramid r,r), ,ho ^.^ ^^
brncbvpinBcoid a:Poo(71, ■ c .oj f
on.l tho boMl rinncoid or(;'). Another inatance is fig. 124 of
a licrrito crystal, whoro tho brachyi.risin «nd pyranuJ combine
MINERALOG?^
aei
fffththemacrodome, of odI'2, P.tPw. - The above figures are rery
common forms of bar}'(ts,— figs. 125 and 126 being both composed
of the pinacoid OP, a brachydome, and a macrodome, with sign
)P(c), ?ao (/), iPco (d). The variation in aspect arises from the pre-
dominance of different faces ; and fig. 127 consists of the macrodome
vPflo,. the prism. «>P(j), and the pinacoid OP.
Dblique V.'The Oblique Prismatic System. — This system is char-
prismatic acterUed by. thr^e unequal axes, two of which intersect
system, -j^ch other at an oblique angle, and are cut by the third at
right angles.ftOne of the oblique axes is chosen as the
chief axis, and the other axes are then distinguished as the
orthodiagonal (right-angled) and <:linodragonal (oblique-
angled). \^The same terms are applied to the chief sections,
and the name of the system refers to the fact that these
two planes form with the base two right angles and one
oblique angle C.
^ The fortPLof this system approach very near'to those of the right
prismatic series, but the inclination of the axis, even when almost
h Bridal & right angle, gives them a peculiar character, by which they are
■ character, ahrays readily distinguished. : Each pyramid thus separates into
tw- altogether independent forms or hemipyramida.
I Prisms, Three varieties cf prism also occur — vertical, inclined, andnori-
zontal — with faces parr.Uel to the chief axis, the clinodiac;onal, or the
orthodiagonal. The horiiontaV
prisms, like the pyramids, sepa-
rate into two independent partial
forms'namedhemiprisnisorhemi-
domes. The inclined prisms
are often designated clinodomee,
the tcrm_ prism being restricted
to the vertical forms. Ortho-
pinacoids and clinopinacoids
are also distinguished, from
their position in relation to
the aXea. , The monoclinic pyra-
mids (fig. 128) are bounded by
eight scalene triangles of two
kinds, four and four only being
similar.* Their lateral edges lie
all in one plane, and the similar
triangles are placed in pairs on
the clinodiagonal polar cti^es. -^
•f snd- The two pairs in the acute angle' between the orthodiagosal and
pyramids, basal section9''are designated the positive hemipyramid, whilst the
two pairs in the obtuse angles of the same sections form together.
the negative hcmip}Tamid. But, astheaehemipyramids are 'wholly
independent of each otlier, they are rarely . observed combined,
llofe frequentlj' each occurs alone, and then forms a prism-like
'figure, with faces parallel to the polar edges, and open at theextrenii-^ ;
ties,*- Hence, like all prisms, they can only appi
CJ. ^c4
Fig. 128.
with other foriQt.^ The vertical iirisma are bounded by four equal
faces parallel to the principal axis, and the cross section is a rhombus ;
the cUnodomes have a similar* form «nd section; whilst the hori-
zontal prisms or. domes have unequal -faces, and their section is a
rhomboid. ^
I' The mode~of derivation of these forms closely resembles that of
the rh<;imbic series. A complete double pyramid is assumed as tie"
fundamental fbnn, and designated ±P, in order to express the two
-portions ol which it consists. Its dimensions are given when the
proportion of its zxes a:b:c and the angular inclination of the
oblique axes C, wliibh is also the inclination of the orthodiagonal
section to the base, are known.
•_The fundamental series of forms is OP .... ±mP . . . . iP
'. . .*.±jnP. ... 00 P, from each of whoso members, by changing
the dimensicxns of the other axes, now forms may be again derived.
Thus from ±jnP, by niuUiplying^tho orthodiagonal by any number
ti, a series of orthtfpyramids ±mP°ii is prpductd, with the ortho.
domes mP'oo as limiting forms. The clinodiagonal produces a
similar series of clinopyramids dbmP'H, with the limiting clinodome
WiP'oo always completely formed, and therefore without the signs
k: attacjied. From ooP arise orthoprisms ocP'n and the ortho-
pioacoid t»P'«o. and clinoprisms ocP'ii and the clinopinaeoid
> or e attached to the P indicates til
Fig. m represents a very common form of gypsum crystals,
OOP <o, (Py, ooP(/), P(J). Tie „,„3t common form of augiteis repi^-
sented m fig. 130, with the sign ooP(i/), ooP'oo(r), ooP'»(;),P(,).
Fig- 131. ug. 132.
Fig. 131 is a crystal of common felspar or orthocbse, composeaoftht
clinopinacoid <x>Va>{M), the priajii;ooP(r), the basal pinacoid
0?{P), and the h«nidoines 2P*oo'(y);to which, in fig. 132 -of tin
same mineral, the hemipyramid P(o) and the clinodome 2P.'oo (ii) are
VI. Anorthic iOrr Triclinic System. — Tlii3'is-< the "least Anorthin
regular system, and departs the most widely, indeed almost system,
absolutely, from symmetry of . form. «^ The axes are all
unequal, and inclined at anglfcs none of which are right
angles, — so that, to determine any ci^stal, or series of forms,
the proportion of the axes a : b : c, afid also their angles,
or those of the inclinatioa of the chief sections, must, be
known. As in the previous systems, one axis is choseii as
the principal axis, and the two others distinguished as the
.. macrodiagonal and btacbydiagonal axes. In consequence
in combination "* of the oblique position of the primcipal sections, thi? system
consists entirely of partial forms wholly independent of
each other, and each composed only of two parallel faces.
The complete pyramid'is thus 'broken up into four distinct
quarter-pyramids, and the prism into two hemiprisms.
Each of these partial forms is. thus nothing more than a,
pair of parallel planes, and the various forms consequently
mere, individual faces. This- circumstande rendei-s many
triclinic crystals very unsymmetrical in appearance.
Triclinic pyramids tfig. 133) are bounded by eight triangles trbosf
lateral edges. lie in one plane. They
are equal and parallel two and two
to each other, each pair' forming, aa
just stated, a tetartopyramid or open
form, only limited by combination
with other fonus, or, as 'we may sup-
pose, by the chief sections. The prisms
are again either vertical or inclined ;
the latter are named domes, and their
section is always rhomboidal. In deriv-
ing the forms, the fundamental jiyramid
is placed upright with its brachydiagonal
to the spectator, and the partial
Fis.133.
P*ooT*'In these signs the _ _ __, _ ,
the orthodiagon.ll (o) or clinodiagonal (c) axis has been multiplied., j forms designafed, the'two upper' by 'P
Formerly the latter forms were enclosed in brackets, thus (mPoo)j and P'. the two lowel- by ,P and.P,, as
»=mPflo.„.^, .,, 1 in the figure-. The further derivation
•» Tlic combinations of this system may be easily understood from now follows as in the right prismatic ^sysjetn; vflth thejn<rd!£ca
their rcsemhlanco to those of the right iirismatic. the chief difficulty . tions already mentioned. _^
being in ^he occurrence oi parlial forms,, which, however, closely : Some combinations of this'sj'stem," as the series^'exhibited'ljy
resemble, the hcmilicdral forms of the previous systems.fA f«w^) most of the felspars, approach very near to the oblique prismatic
examples only need therefoi-c be given..*^ ^ystem ; whilst other*, as cyauose and axinite, show great income
862
MINERALOGY
pleteness and want of symmetry. In the latter case the determina-
tion of the forms is often difficult. In the albite crystal (figs.
134, 185) P is the basal pinacoid OP ; M the brachydiagonal
pinacoid ooPoo ; s the upper right pyramid P'; I the right hemi-
priBm ooP' ; T the left hemiprism oo'P ; and x the hemidome 'P'qo .
Figa. 136 and 137 are crystals of axinite, the former from Dauphin^,
Fig. 136.
Fig. 136
Fig. 137.
Oonio*
hieters.
the latter from Cornwall, of whose laces the following ia the de-
velopment : — r the macropinacoid ooPoo ; P the left hemiprism
t ooT; «the left upper quarter-pyramid T; I the left upper quarter-
pyramid 2'P; « the Jeft upper partial form of the macropyramid
3'P3 ; and x the hemidome 2'P'oo .
The Measurement of the Angles of Crystals.
^ The permanence of the angular dimensions of crystals
shows the importance of some accurate method of measur-
ing their angles, — that is, the inclination of two faces to
each other. Instruments for this purpose are called gonio-
meters.
Two have been specially usea for this purpose — the common or
contact goniometer, invented by Caringeau, and the reflecting
goniometer of Wollaston. The fortner is simply two brass rulers
turning on a common centre, between which the crystal is so placed
that its faces coincide with the edges o^ the iiilers, and the angle
ia then measured on a graduated arc. This instrument is suffici-
ently accurate for many purposes and for large crystals, but for
precise determination is far inferior to the reflecting goniometer.
This requires smooth and even faces, but these may be very small,
even the hundredth of an inch ; and, as small crystals are generally
the most perfect, far greater accuracy can be attained.
The reflecting goniometer is represented in fig. 138. It con-
sists essentially of a graduated circle mvi, divided on its edge
into twice 180% or more frequently into half-degrees, the minutes
I being read off by the vernier hk. This circle turns on an axis
connected with tt^ so that by turning this the circle is moved
round, but it is stopped at 180", when moving in one direction, by
a spring at k. The other part of the instrument is intended to attach
and adjust the crystal to be measured. The first axis of vnn is
hollow, and a second axis, aa, passes through it from S5, so that
this and all the connected parts from b to / can bo turned without
moving the circle inm. The axis d passes through a hole in be, so
that it can turn the arm de into any required position ; / is a
similar axis turning the arm og, and jtq a. fourth axis, in like
manner movable in g, and with a small knob at g, to which the
crystal to be measured is attached.
When about to be used, the instrument should be placed on a tabic,
with its base horizontal (which is readily done by the screws in it),
and opposite to a window at about 12 or 15 feet distance, so that
its axis shall be parallel to the horizontal bars of the window.
One of the upper bars of the window, and also the lower bar, or,
instead of the latter, a white line on the floor or table parallel to
the window, should then be chosen, in order to adjust the crystal.
The observer places himself behind the instrument with the side a
at bis right hand. The crystal is then attached to y by a piece
Af wax, with the two faces to bu measured upwards, and the
edge of union of the faces, including the angle to uo measured, ac
neariy as possible in the lino of aa. The eye being brought near
to the first face of the crystal, the axes aa and p are turned till the
image of the window ia seen reflected in the face with the horizon-
tal and vertical bars in their position. The axis d ia then turned
through a considerable angle
(say 60°), and the image of
the window again sought and
brought iuto its proper place
by turning the axis/, without
moving;?. When this is dom
that face is brought into ita
true position, normal to d, so
that no motion of d can dis-
arrange it. Hence the image
of the window may now be
souglit in the second face, and
brought into its true position,
with the horizontal bars seen
horizontal, by moving the
axes d and a. When this is
done the crystal is properly -^
"adjusted." The angle is
measured in the following
manner. First bring the zero
of the circle and vernier to
coincide, and then turn the
inner axis a or ss, and move
the eye till the imago of the
upper bar of the window re-
flected from the more distant
face of the crystal coincides
with the lower bsr or hori-
zqntal line seen directly.
Keeping the eye in its place,
turn the other axis U till the
reflected image of the upper
bar in the other face in like „. ,„„
manner coincides with the ^^'
lower line ; the angle of the two faces is then read off on the
divided circle. As the angle measured is not directly that of the
faces but of the rays of light reflected from them, or the differ-
ence Iwtween the angle wanted and 180", the circle has the degrees
numbered iu the reverse direction, so as to give the angle without
the trouble of subtracting the one from the other.
The apparatus figured is for adjusting the crystal, and is an im-
provement suggested by Nauraann. In the original instrument the
axis fo was made to push in or out in a sheath, and had a small
brass plate, bent at right angles, inserted in a cleft at o, to which
the crystal was attached. The crj-sUl was adjusted as formerly by
moving the plate, or the axis fo, and by slight motion of the arm
de, which should be at right angles nearly to be when used. A verr
marked improvement is to have a small mirror fix'ed on the stand
below the crystal, with its face parallel to the axis oa, and inclined
at 45° to the window, when the lower line can be dispensed with,
and the instrument used for various other purposes of angular
measurement. Many more perfect instruments have been intro-
duced for the purpose of insuring greater accuracy ; but the simple
instrument is sufficient for all purposes of determinative mineralog>',
and the error from the instrument will, in most casc§, be less than
the actual variations in the angles of the crj-stals.
Departure from Geomdric Simplicity and Loss of
Regularity in Crystals.
Such departures may be regulated by law, or may result
from an undue operation of the force of accretion in certain
directions.
1 . Regular Departures from Simplioiiy. — There are three
varieties of this : — parallel groupings, tmn forms, hemitrope
forms.
Parallel Grojiptngs. — A plurality of individuals are here Cr3fKtal
arranged either so that a line which joins their centres poupt.
becomes a prolongation of one or other of their cry:tallo-
graphic axes, or bo that their axes are parallel.
Fig. 20 shows the first, where cohesion sufficient for stability
requires that the minute octahedra must mutunlly penetrate some-
what into each other. Fig. 139 shows the same in boryte. If wa
suppose octahedra united, the upper loft-hand face of the one
with the lower right-hand face of the other, there would be
parallelism of their axes. Kc-entering angles would, in such
cases, prove a plurality of individuals, but if a number of cubes
were superimposed in nimilor position, no such angles would occur,
an elongated square prism resulting; and such arrange Jicnta, if
MIEEEAIOG Y
363
repeated, are linear, or, with diminishing size in the individaal,
acicular.
Fig. 139. Fig. 140.
Dipfez ^loins and Hemitropes. — Though closely related, formed
•rystals. tmder the operation of very similar laws, and to a certain
extent passing into one another, these are not the same.
In the first case a plurality of individuals must be present ;
in the second this is not necessary. In fig. 140 two
indi\-iduals evidently intersect one another; in figs. 141,
142 one individual may be supposed to have been bisected
in ~a certain direction, and the two halves reattached, but
!in a position differing in some definite manner from their
(jelative position before the separation.
Fig. 141. Fig. 142.
TarieCieB » There are four varieties of true twins: those of apposition, of
3f (^ini. intersection, of partial or completed interpcnetration, and of in-
corporation.
The first is exemplified by spinel, as in fig. 143 ; the second by
If,
1
»
/••• \
M
1 ^
K ' ' '
\ • /
' N. ■- HI
[J
\ - /-
i\ ,
-\->
j
Fig. 144.-
Fig. 145. Fit;. UG.
■tnoTolite, as in ft;;. 144; tb« third by catcitc, ns lu fig. 146, and
\)j bleudc, a» iu fig. 145, where tho two inJividuah of tig. 143 may
be supposed to have been forced vertically into one another ; and^
the last by quartz, as in fig. 147.
The foUowing are the laws of unfon of twins. 1. Tlie face of Laws ot
union of twins, termed the "face of composition," must be either twinning.'
a plane which does occur in the mineral twinned, or which can
occur in accordance with the fifth law of symmetry. A face of
Fig. 147. Fig. 148.
union in twins is also a face of union in hemitropes of the same-
minerah 2. From the above it results that the axes of the united
crystals are either parallel {fig. 148) or inclined (fig. 149). .The
former generally occur among
hemihedric forms ; and the two
crystals are combined in the exact
position in which they would be
derived from or would reproduce
the primary holohedral form. The
class with oblique axes occur both
in holohedric and in hemihedric
forms; and the two individuals are
then placed in perfect symmetry, in ^
accordance with law 1.
Twins are generally recognized
by having r«-entcring angles (figa.
150, 151); but sometimes tho
crossed faces coincide in one plane,
when the combination appears as a
single individual {figs. 152, 153).
The line of union may then be im-
perceptible, or it may be disclosed by the intersection of two sets aj
striie (figs. 154, 155), or by some physical diversity in the char;
acters of the two faces.
The formation of twin crystals may be again, or many times;
repeated, — forming groups of three, fonr, twenty-four, or more.
"Wlien the faces of union are parallel to each other, the crystals fonr
Fig. 149.
Fig. 150. ^ Fig. 151.
rows of mueterminate extent.. "When they are not parallel, they
may return into each other in circles, as in rutile; or form bouquet
or rosette groups, as in chrysoberyl (fig. 1561 ; or stellate croups, as
in calcite (fig. 157) and in cerussite (figs. 158, 159).
Fig. 152. x-ig. 153.
When the crystals .iveof different size, greater complexity results;
but a number of minute crystals are frequently arranged upon a
larger at those points where the angles of a single large crystal
would protrude. Occasionally a aimple foxm ia twinned with a
more complex one, as in chabaaite [fig. 160).'
364
MINERALOGY
tropes.
Hemitrope crjrstals we may imagine as haviag been formed from
fl aiDRle crystal, which has been cat into two halves in a particular
direction, and ono half turned round 180°, or 90*, or 60°. The
line about which the revolution is supposed to take place is called
the "axis of revolution." From the amount of turn usually being
180*, Haiiy gave the name hemitrope. The position of the two
Fig. 157. Fig. 156.
halves in this case resembles that of an object and its ima^ in a
mirror, whose surface then would represent the plane of reunion,
tawi J , The following are the laws of hemitropes. The axis of revolution,
leml- ^ always a possible crystalloOTaphic line,— either an axis, a line
tropism. parallel to an axis, or a normal to a possible crystalline plane. The
plane normal to the axis of revolution is called the
twin plane ; it is either an occurring or a possible
plane, and usually one of the more frequently re-
curring planes. Both the axis and the twin plane
Fig' 158. Fig. 169.
bear the same relation to both halves of the crystal in their re-
versed positiqus : consequently the parts of hemitrope crystals are
eymmetrical witn reference to the twin plane (except in triclinic
forms and some hemihodral crystals). ' The face of composition
veiy frequently coincides
with the twin plane ; when
not minciding, the twin
plane and the face of cora-
posilion are generally at right
angles to each other, so that
the compubition face ia
paiMllnl to the axis of re-
volution. But in twins of
incoj'poration the surfaces of
composition have exercised
a disturbing influence on one
another, so that the surface
of uuion is exceedingly ir-
reguhir. Still in these cases
the axis and the plane of
twinning retain a definite Fig. 160.
positioD ; but the face of composition, being no longer defined, ia
useless as a determinant.
Modes of There are three modes in which the compo. ition may take place
»mion. in hemitropes. These may be explained ly dividing a crystal into
halves, witn the plane of division vertical, LJid then turning one of
the halves round.
Fig. 161.
Fig. 162.
1. One of the halves may be inverted, as if by revolution through
180° on a horizontal axis al right angles to the platte of section, and
'the two faces again united "by the surfaces which were separated.
Here the surfaces of union are the original ones but the base of
one of the halves has -taken the
place of its summit. Examples :
selenite (fig. 161) and orthoclase.
2. One of the halves may be
turned round through ISO', as if
by revolution on a horizoTUal axis',
paralUl to the plane of section, and
the face opposite and parallel to
that of the plane of section — an
originally external face— may then
be applied to the other half. Here,
not only has the base of one-half
become a summit, but a lateral
and external face of the original
crystal has been thrust to its
centre so as to become a face of
internal union. Example: labradorite (fig. 162).
3. One of the halves may be turned round through 180*, as if by
revolution on a vertical axis, parallel to the plane of section, the
external face opposite and parallel to the plane of section becomin^:r
a face of union. Here, however, both the original summits retain
their position "as summits. Example: orthoclase.
The first 'of these modes of composition may occur in each of the
systems, but it is not always apparent until disclosed by optical
properties. The second is rare, and the third still more so.
In hemitropo crystals (less frequently in true twins) "the
halves of the crystal are frequently reduced in thickness in the
direction of the ordinary twin axis ; and when there is a parallel
repetifibn of hemitropes, which frequently occurs, they are often
reduced to very thin plates, not the thiclmess of paper, giving to
the surface of the aggregate a striated structure ana appearance.
In the cubic system the faces of composition, both of twinning Twits oi
and of hemitropic revolution, are those of the cube, the dodeil^hed- cubic
ron, and the octahedron. systein.
In the first case we have the axes of the two crystals necessarily
in some cases parallel, or, more correctly, falling into one ; but, as
in this system all the axes are alike, or all the cubic faces similar,
composition may occur along or parallel to all alike, and double or-
triple twins occur. We have examples in twins of the pentagonal
dodecahedron (fig. 163) made up by the interpenetraticm ofa right
Fi^. lea Fig. 164.
and a left ( + and - ), and of the tetrahedron, as seen in pyrite
and fahlerz respectively. In virtue of the position required by law 2,-
it will be seen that the position of the solid which is common to
both intersecting crystals is" in the twin of pyrite the four-faced
cube, which is the holohedral form of the pentagonal dodecahedron,
while in the case of the fahlerz twin (fig. 164), the common por-
tion is an octahedron, the holohedral form of the tetrahedron. "^
Fig. 165. Fig. 166.
Twinning on an twtahedral face is seen in the" apposition twin of
spinel (fig. 143), the tetrahedral twin of blende (fig. 165), the inter-
penetrative octahedral twin of blende seen in fig. 166, and the inter-
secting cubes of lluor (fig. 167).
This Ib qIbo the usual twin face for hemitropes of the cubio systeip.
MINERALOGY
365
It ifiieit in fig. 168 of blende, where the two parts of the rhombic
dodecahedron are united by it Magnetite, apinel, and diamond
Tetra-
gonal
twills.
Fig. 167. ^'S- 1^8-
frequently occur in octahedral hemitropes o! tho same composition
This is also the face of composition for tetartohedral hemitropes.
Fig. 170 is that of the diamond. Here six o£ the faces of the six-
Pig. 169. Fig. 170.
faced octahedron, with six faces diagonally opposite, form a low
double six-sided pyramid (a portion of an octahedral face truncating
each) through an 180° revolution of one set of these. Garnet some-
times shows both twins and hemitropes of the dodecahedron, of
dodecahedral composition.
In the Utragcmal sysiem^ twin crystals are very uncommon, but
hemitropes frequent. With parallel axes they very seldom occur,
but are seen in chalcopyrite. "When the axes are inclined, the
plane of union is usually one of the faces of the primary pyramid ;
and, as these faces are all similar, composition may take place
dmnltaneously parallel to all. Very complicated forms hence result,
as seen in chalcopyrite and in cassiterite Cfig. nil-
twins are generally formed by the interpenetration of two rhombo-
hedrons, a + and a - , thB vertical axis being the axis of composi.
Idon; as in chabaaite (fig. 176), cinnabar, levyne, calcitc, &c. Some
times six or more crystals, united parallel to the prismatic olanes.
Fig. 171 Fig- 172-
In cassiterite the plane of union is frequently one of the faces o{
the pyramid Poo , sometimes one of those faces that replace the
polar edges of P (figs. 172 1^). From the bend the latter form
is termed genicolated.
Bexa-
(oul
twins.
Fig. 17S. Fig. 174.
Hausmannite occurs in hemitropea of the primary P ; and on tho
|)olar edges of this other twins are symmetrically repeated, a central
individual appearing like a support to the others (figs. 174, 175).
In the hexagonal system twins are very common among the
rhombohedral (the hemihedral) and the tetartohedral forms; while
hemitTDpes prevail among the hexagonal or holobedral forms. The
Fig, 175. Fig. 176.
form rosettes; as in cbabasite from Giant's Causeway. The almost
endless stellate forms of crystals of snow are built up in this manner.
Many of the most beautiful combinations to be seen among crystals
result from thb mode of arrangement.
Parallel groupings of hexagonal prisms also occur, as in apatite
Rock crystal, in consequence of the tetartohedral character of its
crystallization, exhibits twins in which the double hexagonal
pyramid P may be said to be separated
into two rhombohedrons P and r; these,
though geometrically similar, are physi-
Fig. 177. Fig. 178.
cally distinct. In fig. 178 the two individuals have not entirely in-
terpenetrated, and might be regarded as simply grown together
witn parallel axes; but in fig. 147 there is so complete an inter-
penetration that the composite character of the crystal is only evi-
denced through a difference in the character of the surfaces of the
two halves, which are most irregularly disposed.
The hemitropes of this system often form regular crystals, wien
the two halves have been united by a plane parallel to the base, so
as to appear like a simple crystal,
as in fig. 179. Here each end
shows the forms ooP, - JR, but
the terminal faces appear in
parallel instead of alternate posi-
tion. Something of the same is
seen in fig. 180, a hemitrope
scalenohedron from Derbyshire.
Hemitropes with the face d the
primitive rhombohedron a; the
lace of composition are also '-ora-
mon ; and they are somriimes
joined by a face of - JR, tb ■ two
axes forming an angle of 12/ 34'.
Occasionally a third individual
is interposed in a lamellar f>irra,
as in fig. 181, where the faces
of the two outer portions become
parallel. This is found in some
pieces of Iceland spar. VvTien
the crystals unite in a faoe of
the primary rhombohedron, they
form an angle of 89° 8'; hemiti-jpes
on this law are easily recognised
by their differing so little from a
right angle in the re-entering
bend (figs. 182, 183).
The faces which in this species
act as faces of composition are
Fig. 181.
exceedingly numerous ;. other examples are figs. 142, 146, 148, and
149.
In the right prismatic system twin crystals with parallel axes are lOgtt
rare, but with oblique axes common, the faces of union being one of [-/ismatic
the faces of the prism ooP. Twins of this kind occur freauently m twins.
868
M.I N E R A L 0 G Y
Of Deta-
iled ron.
or do-
deca-
hedron.
rry»^Hl *^r ;ieedle, da happens in red copper and/'pyritea. Cry&Uls
of acicular pyrites occur at the Newton-Stewart lead-mine.
An octahedron flattened parallel to two of its faces is reduced to
ft tabular crystal (fig. 210). If lengthened iu the same direction,
it takes the form
in fig. 211 ; or if
it is still further
lengthened, to the
obliteration of
two opposite octa-
hediJil faces, it
becomes an acute
rhombohedron
(same figure).
Whea an octa-
hedron is extend-
ed iu the direction
of a line between
two opposite
edges, it has the
general fovm of
a rectangular
octahedron ; and
still further ex-
tended, as in fig.
212, it is changed
to a rlionibio
prism with dihe-
dral summits.
The figure ropre-
sents this prism lying on its acute edge (spinel, nuor, magnetite).
Tlie dodecahedron wlien lengthened in the direction of the up-
right axis becomes a S'luarc prism with pyramidal summits (fig.
213); and when shortened along the same axis it is reduced to a
square octahedron with truncated basal angles (fig. 214). Both
Fig. 213. Fig. 214. Fig. 215.
these forms are modifications of ^lic square prism; the first mode
of tlibtorti'ia is common in garnrt, i-emlering it liable to be con-
sidered zircon ; the second is seen in aplome, wlun it might be taken
FiR. 216. Fig. 217.
for stannite. When the first of these forms is flattened, as in fig. 215
it rcycmbles a form of stilbite.
"Wlicn a dodecahedron again is lengthened along a diagonal
between the obtuse solitl abgles, it becomes
a six-sided pnaijn witih trihedral summits,
as in fig. 216; aud when shortened in the
same direction, it becomes a rhombohedron
which has its eix acute 'angles truncated
(fig, 217). In the first
case, a crystal of green
garnet or uwarowite
would resemble diopt
in the latter, coloui
^rnct would resemble,
tiilcile.
Trapezo- The trapezohedron is
hcdron. exceedingly subject to
dfstortions, which fre-
quently disguise it much.
When elongated in the
direction of the upright
Fig. 219,
Fig. 218.
it becomes a double eight-sided pyramid with four-sided
iummHa (fig. 218) ; a further elongatioa along the same axis would
result in the obliteration of these summit faces, and in the produc-
tion of a perfect double octagoiial pyramid (fig. 219), The first
of these distortions is exceedingly common in analcime and not
Fig. 220.
Fig. 221.
nncommon in garnet; the latter rarely occurs in analcime. Length-
ened along an octahedral a^s it becomes fig. 220 ; shortened along^
the same it becomes fig. 221, Both are seen in analcime.
Fig. 223.
Fig. 222.
When the tetrakishcxahedron is len^hened along a single octa- Of tetf**
hedral axis it assumes the form of fig. 222 ; still further elongated, kisheza*
with obliteration of one half of. its planes, it becomes a scalene do- hedron.
decahedron, resembling the "dog tooth" form
of calcite (fig. 223). Fig. 224 is a hemihedron of
tliis form, produced by shortening along an
octahedral axis, with obliter.ition of all the
planes which do not touch the poles of that axis.
In the case of modi-
fied crystals of this
system the distortions
are more complex.
Fig. 225 represents a
crystal of cinnamon-
stone from Aberdeen-
shire; it is a con^bina-'
tiou of the dodecahe-
dron and the traj^ezo-
hedron. Only four
dodecahedrnl faces re-
main {d), and those
Fig. 224.
Fig. 225.
trapezohedron (") are of unequnl size. It may be best
understood by regarding it as fig. 21S with the four vertical faces
of fig. 213 ; so that it combines the distortions of both of these
figures.
Crystals of dinmond are very frequently distorted, though gene-
rally through curvatures of their faces.
Imperfections in the Surfaces of Crystals,
Of these the most important are strife, caverns, and
curvatures.
1. Strutted SirrfaccB. — Tho jmrallel furrows on the surfaces oflmperf^
crystals are called istrin?, ondKuch aurfocea arc said to be btnated. tion of
Each ridgo on a striatod surface is cncloaod by two narrow planes. surfaceiL
Those planes often correspond in position to i secondary or to the
primary plnnos of the crystol, and ■we may eunposo these ridges to
havo been formed by ropontod opc-ill/ition in toe operation of those
causes which give rise, when acting uninterruptedly, to larger
planes. By this moans tho surfaces of a crystal are markod'^in
parallel lines with a sucoea^iou of narrow plaucg, meeting at angles
allernately re-ontoring and salient, and conytituting tho ridges
relerred to. Tl>is combination of dilTercnt pl;tno3 in tne formation
of a surface has been termed an oscillation of ficos.
Cubes of pyrites are gonorally striated in buch a way that the Striatloo.
striffl on adjorent faces are at right angles to one another. These
lines are parallel to the intcntectiona of the primary faces with the
planes of the pentagonal dodecahedron, whicn is the most common
torm of pyrites ; and they have evidently resulted from an oscilla-^
tion between the primary and this secondary form.
The rhombic doaecahedron 1& often striated parallel either with the
MINERAJLOay
36&
edsea. or with the longer or the shorter diagonal of its faces. In the
irScase, seen in ganiet (flg. 226), there w a Mfisage into the »ii-
faoed octahedron ; the second results from an oscUlatory combination
'of the dodecahedron with the regular octahedron, as in magnetite ;
and the last with the cube, as in eplome.
Rhombohedrons of chabaaite are often rtnated parallel to the
Fig. 226.
y>e. 227.
in the left-handed and right-handed crystals, the twist i/t to the
right or left according as the crystal is right- or left-handed.
The surfaces of crystals are frequently far from flat, on accoont of
fracture, with dislocation of the several fragments, occasioned by
motion in the enclosing rock, the material of which is forced, or it
may be transfused, into the rents. The tourmalines and beryls (fig. Dislo*
234) which occur in granitic dykes are very subject to this, the frag- cated >
menu being often bent as well as displaced, A more or less siDiul- crystida
tancous eflbrt in the crystallization of two substances may produce
a structure with the external form of one, the interior of which
exhibita imbedded crystals of the other, more or less perfect in
their development. In pegmatite or graphic granite, rude crystals
of felspar contain skeleton forms of quartz, of which generally only,
one side of the prism and two of the pyramid occur, forming a radi»
lettering. Similar hollow quartz forms occur imbedded in gameV
radiating from its ceutre (fig. 235), and roughening its surface from
protrusion, without distorting ita form. Totally imbedded micro-
scopic crj'stals, "microliths," are, as in the latter cases, chemi'!
terminal edges (fig. 227), indicating an oflcillstory combination be-
tween the primary facea and a secondary plane which, bevels these
edges. _
Striation effaces is more frequent in the rhombohedrsd system
than in any of the others. Horizontal stris are of almost invariable
occurrence is the prismatic
faces of quartz, whatever be the
form of the crystal. The oscil-
lation hero has taken place
(between the pyramidal and the
'prismatic faces (figs. 228, 229,
230). During its growth there
seems to have been a con-
tinued efibrt to complete the
'crystal by the assumption of
the terminal planes, — which
effort was intermittently over- F'g- 228. Kg. 229. Fig. 230.
come by a preponderating one to continue the deposition of matter
along ita main axis. Quartz crystals, from these alternate efforta,
<^n taper to a point, without having auy regular pyramidal face.
The lateral planes of prisms of tourmaline are very frequently
•onvex, owing to oscillation between several lateral faces. In all
such cases the interfacial angles cannot be determined, as they ar«
lost in the rounding.
The striatiooa on the lateral faces of fbliated minerals are merely
the edges of laminse. Examples : mica and gypsum.
QiTsrft^ 2. Cavernous Crystals. — Ci7stals not unfrequently occur with a
•nafacas. deep pyramidal depression occupying the place of each plane, as is
often observed in common salt, galena (fig. 21), and sulphur. In
the solution of crystals through atmospheric exposure, an approach
to the same form is sometimes obtained, owing to the fact that the
centres of the faces yield sooner than the edges and angles. Crystals.
of redmthite are often thus cavemoos. Sometimes octahedrons
occur with a triangular cavity, in place of each face (fig. 22). The
same is met with in other forms.
Oarred 3. Curved Surfaces. —Curved surfaces sometimes result from the
nrfacesT'oscillatory combination already noticed. Otners result from a
curvature in the lamin.-e constituting the crystaL Crystals of i
diamond have convex faces, and are sometimes almost spheres. I
Tliis modo of curvature, in which all the feces are equally convex, I
is less common than that in which a convex surface is opposite and I
parallel to a corresponding concave surface. Rhombohedrons of
spathic iron and pearl spar are nsuallv thus curved, as is shown
iu fig. 231. The saddle-shaped crystals of the same mineral (fig.
Fig. 234. Fig. 236.
cally non-assimilable. These are frequently arranged in lavers in
the including crystal, as in augite-anJ leucite. 'When tnere is
a certain amount of chemical resemblance there may _ occur a
definiteness in the arrangeHient ; and if the enclosed substance
crj'stallizes in a system differing from that of the mineral which
includes it, the angles of the latter are more or less distorted. This
is the case in " microcline," where the intrusion of a plagioclastio
felspar causes some departure from the rectengularity of orthoclase.
Foreign amorphous matter caught up or attaching itaelf to the
surface; of a crystal, duringthe process ofits growth, causes lines of
feeble cohesion, — as in the case of capped crystals of quartz. Here
an occasional selectiveness in the seta of faces to which the foreiga
matter adheres seems to indicate that it has been to some extent
under the influence of a polarity in its adhesion. Something of the
saine kind seems to have influenced the srrangement of the quartz
grains caught up during the formation of the crystal of garnet
shown in fig. 236. The perfect modelling of rock crystals is,
however, but little interfered with by the almost numberless
substances which they contain.
^ggrerjaiion of Cryttalt.
Crystalline aggregates which pass into amorphous masses
may, in their more marked or perfect form, be assigned to an
imperfect twinning.
Fig. 231. FiK 232. I Crystals are often grouped in linear series, as in iiative Regular
«,o> .,.„„'.,',.. . , , . , ' copper and silver, and thus constitute long threads or re- aggre-
232) are remarkable instances of several reversed curvatures in the f,•„,,Io^;/^„o t„ »i„ * . j _. . i ^i. i- ■ • i, ,.1. i?atiM
».me face. A sinmlar curvature is shown in fig 233, of cilcite: ^^""^^^"^^^ ^ clustered crystals those adjoining each other S'^'"-
The conical erj'stals of brown zinc blende, aud the lenticular and "^ generally parallel in position, and are muted by a
conical crystals of gypsum, are other examples. Crj-stals of plane parallel to one of the principal sections, or to planes of
a.uartzare sometimes curved and twisted. When this takes j.hico common occurrence. Senarmont mentions a union in galena,
868
M. I N E R A L 0 G"Y
Of octa-
hedron.
Of do.
deca-
hedron.
crystr'l or ."leeJlc, aa happens in red copper and/ pyrites. Cry&L^lo
of acicular pyrites occur at the Newton-Stewart lead-mine.
An octahe-iron flattened parallel to two of its faces is reduced to
a tabular crystal (fig. 210). If lengthened iu the same direction,
it takes the form*
in fig. 211; or if
it is still further
len;(thened,tothe
obliteration of
two opposite octa-
hf^dral faces, it
becomes an acute
rhombohedron
(same figure).
A-Vhea an octa-
hedron is extend-
ed iu the direction
of a line between
two opposite
edges, it h;is the
general form of
a rectangul.ir
octahedron ; and
still further ex-
tended, as in fig.
212, it is changed
to a rhombic
prism with dihc- //J-
dral summits. ^. 212.
The figure ropre- ° °
sents this prism lying on its acute edge (spinel, fluor, magnetite)^
The dodecahedron when lengthened in the direction of the up-
right axis becomes a square prism with pyramidal summits (fig.
213); and when shortened along the same axis it is reduced to a
square octahedron with truncated basal angles (fig. 214). Both
Fig. 213. Fig. 214. Fig. 215.
these forms are modifications of 'he square pri.sm; the first mode
of distortion is common in garnft, i-eudering it liable to be con-
sidered zircon ; the second is seen iu aplome, wlu-n it might be taken
Fi(r. 216. Fig. 217.
forstanuiti'. When the first of these forms is flattened, as in fig. 215
it resembles a form of stilbite.
When ft dodecaliedrou again is lengthened along a diagonal
between the obtuse solid angles, it becomes
a six-sided prisyi witti trihedral summits,
as in fig. 216; and when shortened in the
same direction, it becomes a rhombohedron
which has its six acute
(fig. 217). In the first
case, a crystal of green
garuct or uwarowite
would resemble dioptase ;
in the latter, colourless
f^rnct would resemble^
^ilcile.
Tr»pezo- The trapezohedron is
hedron. exceedingly subject to
dfetortions. which fre-
quently disguise it much.
When elongated in the
direction of the upright
Fig. 219.
Fig. 213.
axia it becomes a double eight-sided pyramid with four-sided
flummita (fig. 218) -, a further elongation along the samo axia would
result in the oblitention of these summit faces, and in the produc-
tion of a perfect double octagonal pyramid (fig. 219), The tirst
of these distortions is exceedingly common in analcime and not
Fig. 220.
Fig. 221.
uncommon in garnet; the latter rarely occurs in analcime. Length-
ened along an octahedral axis it becomes fig. 220; shortened along
the same it becomes fig. 221. Both are seen in analcime.
Fig. 223. Fig. 222.
"WTien the tetrakishcxahedron is lengthened along a single octa- Of tetft*
hedral axis it assumes the form of fig. 222 ; still further elongated, kisheia-
with obliteration of one half of its planes, it becomes a scalene do- hedron.
decahedron, resembling the *'dog tooth" form
of calcite (fig. 223). Fig. 224 is a hemihedron of
this form, produced by shortening along an
octahedral axis, with obliteration of all the
planes which do not touch the poles of that axis.
In the case of modi-
fied crystals of this
system the distortions
are more complex.
Fig. 225 represents a
crystal of cinnamon-
stone from Aberdeen-
shire ; it is a conkbina-'
tiou of tho dodecahe-
drou end the trajwzo-
hedron. Only four
dodccahedrnl faces to-
maili (rf), and those
of the trapezohedron (h)
understood by regnnling it ns fig. 218 with th6 four vertical ftrces
of fig. 213 ; so that it combines the distortions of both of these
figures.
Ciystals of diamond are very frequently dislortedj though gene-
rally through curvatures of their facra.
Imperfectioyis in the Surfaces of Crystals.
Of these the most important are striee, caverns, and
curvatures.
1. Striated S^trfaccB, — Tho jarallcl furrows on the eurfflrea of luperfto.
crybtala ore called atria?, andcuch BurfaccB arc said to be strinted. tion of
Each ridgo on a etriatod suKace is oncloaed by two narrow planes. eurface&
Those planes often correspond in position to t aecoudary or to the
primnry plnncs of the crystol, onu wo may euniwse those ridges to
navo been formed by ropentod o»«.'illntion in tne operation of thow
cousoa which give rise, when acting uninterruptedly, to larger
planes. By this moans tho eurfocea of a crystal ore markoa in
parallel lines with a Bucoo».-.iou of narrow planes, meeting at angles
allernately re-ontoring and salient, and conbtituting tho riagea
relerred to. Tl>ia combination of dilTercnt phinesin tne formation
of a surface has been termed an oscillation of firos.
Cubes of pyrites are generally etriatod in nuch a way thnt the StrUtta^
Btrifle on adjacent faces are at right angles to cue another. These
lines aro parallel to tho intcrsectionfl of tho primarj* faces with the
planes of the peutagnnal dodocnhedron, whicn is the most common
form of pyrites ; and they have uvidently resulted fi-om an oscilla-^
tion between the primary and this secondary form.
The rhombic dodecahedron lb often striated parallel either with the
MINERAJUOU-y
369
edees or with the longer or the shorter diagonal of its faces. lii the
firet cose, seen in garnet (fig. 226), there u a passage into the «ix-
faoed octahedron ; the seconil results from an oscillatory combination
'of the dodecahedron with the regular octahedron, as in magnetite ;
•nd the last with the cube, as in aplome.
Rhombohedrona of chabaaite are often etnated parallel to the
^^%^ dk
Fig. 226. Fig. 227.
terminal edges (fig. 227), indicating an oscillatorjr combination be-
tween the primary faces and a secondary plane which, berels these
edges. _
Striation of faces is more frequent in the rhombohedral system
than in any of the others. Horizontal striae are of almost invariable
occurrence in the prismatio
faces of quartz, whatever be the
form of the crystal. The oscil-
lation hero has taken place
(between the pyramidal and the
'prismatic faces (figs. 228, 229,
230). During its growth there
seems to hare been a con-
tinued effort to complete the
'crystal by the assumption of
the terminal planes, — which
effort was intermittently over- F'g- 228. Fig. 229. Fig. 230.
come by a preponderating one to continue the deposition of matter
along its main axis. Quartz crystals, from these alternate efforts,
<^n taper to a point, without having auy regular pyramidal face.
Tho lateral planes of prisms of tourmaline are very frequently
convex, owing to oscillation between several lateral faces. In all
snch cases the interfacial angles cannot be determined, as they are
lost in the rouuding.
The striations on the lateral faces of fbliated minerals ax« merely
the edges of laminse. Examples : mica and g3rpsum.
CVerei 2. Cavemmis Crystals. — Crystals not nnfrequently occur with a
n» ttiote. "leep pyramidal depression occupying the place of each plane, as is
often observed in common salt, galena (fig. 21), .ind sulphur. In
the solution of crystals through atmospheric exposure, an approach
to the same form is sometimes obtained, owing to the fact that the
centres of tho faces yield sooner than the edges and angles. Crystals.
of redrnthite are often thus cavernous. Sometimes octahedrons
occur with a triangular cavity, in place of each face (fig. 22). The
same is met with in other forms.
OMrred 3- Curved Surfaces. — Curved surfaces soraetiraes result from the
Ivfacesr'osciUatory combination already noticed. Otners result from a
curvature in the lamiure constituting tho crystal. Crystals of
diamond have convex faces, and are sometimes almost spheres.
This mode of curvature, in which all the ff>ces are equally convex,
is less common than that in which a convex surface is opposite and
parallel to a corresponding concave surface. Rhombohodrons of
spathic iron and pearl spar are usually thus curved, as is sliown
in fig. 231. The saddle-shaped crystals of the same mineral (fig.
in the left-handed and right-handed crystals, the twist la to the
right or left according as the crystal is right- or left-handed.
The surfaces of crystals are frequently far from flat, on account of
fracture, with dislocation of the several fragments, occasioned by
motion in the enclosing rock, the material ol which is forced, or it
may be transfused, into the rents. The tourmalines and beryls (fig. Dislo*
234) which occur in granitic dykes are very subject to this, the frag- cated I
meuts being often bent as well as displaced. A more or less Bimul- crj-stsla
tancous effort in the crystallization of two substances may produce
a structure with the external form of one, the interior of which
exhibits imbedded crystals of the other, more or less perfect in
their development. In pegmatite or graphic granite, ruae crystals
of felspar contain skeleton forms of quartz, of which generally only,
one side of the prism and two of the pyramid occur, forming a rud&
lettering. Similar hollow quartz forms occur imbedded in garnet,'
radiating from its centre (fig. 235), and roughening its surface fron»
protrusion, without distorting its form. 1 otally imbedded micro-!
Boopic crystals, "microlithB," are, as in the latter cases, chemi'^
Fig. 234. Fig. 236.
cally non-a<isimilable. These are frequently arranged in layers in
the including crystal, as in augitcand leucite. When wen is
a certain amount of chemical resemblance there may _ occur a
definiteness in the arrangeflient ; and if the enclosed substance
crj'stallizes in a system differing from that of the mineral which
includes it, the angles of the latter are more or less distorted. This
is the case in " microcline," where the intrusion of a plagioclastio
I felspar causes some departure from the rectangularity of orthoclase.
Foreign amorphous matter caught up or attaching itself to the
j surfacer of o crystal, during the process of its growth, causes lines of
I feeble cohesion, — as in the case of capped crystals of quartz. Hera
an occasional selectiveness in the sets of faces to which the foreign
matter adheres seems to indicate that it has been to some extent
! under the inilueuce of a polarity in its adhesion. Something of the
, same kind seems to have influenced the arrangement of the quartz
I grains caught up during the formation of the crystal of garnet
shown in fig. 236. The perfect modelling of rock crystSs is,
I however, but little interfered with by the almost numberless
substances which they contoin.
Aggregation of Cry^ali.
Crystalline aggregates which pass into amorphotis masses
may, in their more marked or perfect form, be assigned to an
I imperfect twinning.
Fig 231. yj- 232 Crystals are often grouped in linear series, as in native Regular
9.«v .„,..„',, V, ■ I , , , ' . , ' copper and silver, and thus constitute long threads or re- »ggre-
ai) are remarkable instances of several reversed curvatures in the f;n„i„«;„„„ t_ i * .. j i i xi. j- • • i. ii. ntpi
• aam, face. A singular curvature is X)wn infig 233 of calcite! ''"^^lations. In clustered crystals those adjoining each other S^'"-
The conical crystals of brown zinc blende, aud the lenticular and ^^^ generally parallel in position, and are umted by a
conical crystals of gypsum, are other examples. Ci-j-stals of plane parallel to one of the principal sections, or to planes of
ftuartz are sometimes curved and twisted. When this takes place common occurrence. Senarmont mentions a union in galena,
870
MIN.EKALOGY
crystal
^owth.
■<lTegul!
aggi'6-
^tes.
< struc
fUre ill
liarallel i'o the octahedral faces, ns coucinon ; and he also
^escribes an instance where -the union was parallel to the
^lane 3f .
The positions of crystals on tLc suijporting'rock seem at firet
(to be without auy regularity. But by closer inspection we detect
even here the same law of harmony that governs the formation of
the simple and compound crystal The various positions assumed
correspond generally with tho more common kinds of composition
in twin crystals. This regularity is not always manifest on account
of the unevcnness of the surface on which they rest. In general,
however, on glancing over a surface covered with crystals, a
Teflexion from one face will be accompanied mth reflexions from
|the corresponding face in each of the other crystals, showing that
the crystals are similarly positioned throughout.
This tendency to parallelism in tho "positions of associated
crystals is apparent even in crystalline aggregates. In granite
for example, which is composed of felspar, quartz, and -mica, the
felspar ciystallizations have usually a common position ; that is
,the corresponding extremities lie in the same direction, or nearly
eo. On this account granite is cleavable in one direction more
easily than in others, and this direction is that of the perfect
cleavage plane of the felspar; the second less perfect cleavage of
the felspar permits of fracture of the rock nearly at right angles to
the first ; but, as there is no such third cleavage in the felspar, the
workman, in fashioning the blocks of granite for paving stones, is
impelled to chip or dress them off in the third direction.
;- The dominant action of polarity may, moreover, give a parallel
Position to the main axes of different minerals belonging to the
.•,ame system, when crystallizing in association, and even to those
which belong to different systems.
Fig. 237 is an illustration of the first
of such cases, whore a crystal of zircon
is implanted into a crystal of xenotime,
and has its main axis identically in
the same line. As illustrations of the
latter — a parallel position of the axes
of crystals of different systems— there
are records of such association in
Crystals of cyanite and staurolite, of
tnuscovite and haughtonite, of albite
and orthoclase. The same has been
observed between crystals of rutile
and specular iron, — the crystals of
I'utile in this case having the vertical
juds in the direction of a lateral axis
ft the specular iron. Haidinger has observed pyroxene and hom-
Hende crystals associated in parallel positions.
A prism of caloite terminating in the planes g (fig. 106) has been
(Observed, in which each plane was covered with small crystals of
fl uarU all lying symmetrically, with their pyramids pointing towards
^he summit of the calcite crystal. When one mineral is chani^ed
into another, a polarity of accretion is still often seen to have domi-
bated m the arrangement. In a crystal of calcite which had been
Bhangcd into a number of minute crystals of aragonite, the main
ftxes of the latter all lay in the direction of the main axis of the
tiiiginal crystal of calcite.
r Irregular Aggregation of Crystals.— Besiaes the regular
"jmons now describe'd, crystals are often aggregated in
p.iculiar ways, to which no fixed Jaws can be assigned. ■ •
Thus some crystals, apparently simple, are composed of concen-
|tr!c crusts or shells, which may be removed one after the other
always leaving a smaller crystal like a kernel, with smooth distinct
pees. Some specimens of quartz from Beeralston in Devonshire
teonsist apparently of hollow hexagonal pyramids placed one within
Another. Other minerals, as fluor-spar, apatite, idocraso, heavy
fepar, and calcrspar, disclose a similar structure by bands of dif-
ferent colours, A growth rendered intermittent throufli tho
ideposition of a thin layer of foreign matter is thus developed.
Many large crystals, again, appear like an aggregate of numerous
small crystals, partly of the same partly of dill'erent forms Thus
some octahedrons of fluor-spar from Schlaggenwald are made up of
pmall dark violot-blue cubes, whose projecting angles give a drusy
character to the faces of the larger form. Such polysjmthctic
fcrystals, as they may bo called, arc very common in calc-spar.
: :I'orms of Crystalline Aggregates. — Crystals have often
been produced under conditions i)rcventing the free de-
velopment of their forms ; and, according to tho direction
of the axis in which the dovelopmeut has been checked,
'|they may be divided into " columnar .'.'- and "lamellar"
arrangements.
Tlie columnar struelure is made up of a mor« or less fibrous
arran-eraent; and this may be supposed to have accrued from the
«mult«iieou« growth of a multitude of cryatals from u .single or
Fig. 237.
from closely adjacent centres of support, eo that, while the crystal,'
were free to elongate themselves in the direction of their main axis,
their increase was restrained laterally, by their impact upon one
another. When the surfaces of support are level, or consist of
the opposing sides of a vein, the columns or fibres, frequently
exceedingly delicate, are parallel, and not unfrequently they then
have a silky lustre. In the latter *f the above circumstances the
fibres are disposed transversely to the vein. Examples: gypsum,
chrysotile, satin-spar. When the surface of support is rough, or haa
angular projections, the fibres radiate from certain of the=c in all
directions, producing, in a thin vein, a starlike form, whence tho
aiTangement is called "stellular." Example : wavellite. AVhenthis
takes place in an open cavity, producingbnish-like forms, they are
termed "radiant." Examples ; antimonite, necdlestone. When the
points of divergent growth are so positioned that the radiating
groups interlace with one another, the structure is said to be
"reticulated," from its resemblance to a net. Example : tremolite.
"When individual members of such fibrous structure project above
the general surface with acuminated extremities, they are said to be
'' acicul.ar"; when the protruding columns are of uniform thickness
they are termed " bacillary," or rod-Like. Such terms as straight,
carved, twisted-columnar, diverging, or confused-fibrous explain
themselves. Such fibrous arrangements as the above may occur
imbedded centrally in a rock mass, which had been the magma
out of which they were formed; or they may line the inner surface
of cavities, filled originally either with water or aqueous vapour.
These modes of occurreece have been distinguished by Hobs as
crystal groups and druses. The former includes all unions of im-
bedded crystals round a central nucleus; the latter those of crystals
of simultaneous or regularly successive growth on a common
support. In the first case, there may be spheroidal, ellipsoidal, cocks-
comb, or other forms, frequently seen in marcasite, pyrite, and
gypsum. In the second, spheroidal forms are less rare, but ar»
seen in the case of several of the fibrous zeolites. In such cases
surfaces more or less rough are coated, and diminished in angularity,
through the hemispherical forms produced by the radiation of L
multitude of fibres. Certain imitative outlines thus result from the
successive deposition of layers of these crysUls. These forms or
uniting masses are termed "globular" when nearly spherical, "botry-
oidal " when like bunches of grapes, " reniform " or kidney-shaped
when the spheres are larger, more confluent, and less distinct, and
"mammillated" when the masses are nearertohemispheres. Mesolite
occurs in globular forms; piehnite in hotryoidal; hamatite and
chalcedony in reniform; and siderite and calamine in mammillated.
In all the above cases the transverse fracture of such structures dis-
closes tlie fib,-ou3 arrangement of the parts ; but, if the giowth has
been intermittent, lines of deposit, concentric with the central
nucleus of each sphere, are evidenced by layers of distinct colours.
1' racture or separation frequently takes place, also, along such lines.
In such drusy cavities— termed "geodes " when they are circular-
after a certain number of such lines of deposit, grouped arrange-
ments which have somewhat more of free crystalline development
may assume other imitative forms in which there is a certain
dependence on the crystallographic character of the mineral con-
cerned. There are thus produced coralloidal or coral-like groups,
tmticose or cauliflower-like groups, capillary or hair-like, and fili-
form or thiead-like or wire-like forms. Often these groups expand
in several directions, and produce arborescent, dendritic plumose
mossy, dentiform, or other forms. Such are common among the
native metals; as gold, silver, and copper. Mesolite is very
frequently plumose. A "drusy crust" is the term applied to a
thm rough layer of crystals, which invests either a large crystal
or the surface of some other body lodged in the interior of
cavities.
In tho lamellar structure a development along the main axis
would apjjear to have been checked, and tho crystallographic force
to have expended itself laterally; though this is not the invariable
habit of a species under all circumstances, as exemplified by baryte.
This structure consists of flat crystils, plates, or leaves. It is
termed "tabular" when tho plates are of uniform thickness,
"lenticular" when they are thinner on the edges, "wedge-shaped"
when sharp on one edge, "scaly" when the plates are thin and
small, " foliaceous" when larger and easily separable; " micaceows"
IS also used to describe this kind of structure. It may also be curved
lamellar and straight lamellar. Wollastonite, when flat lamellar,
13 called tabular spar ; gypsum is frequently lenticular, Ulc scaly.
Lamellar minerals when radiating from a centre 6rten form fan-
shaped, wheel-like, almond-shaped, comb-like, and other groups.
In tho granular structure, the force of crystallization has been
exerting itself along all the axes ; but, from the multiplicity of
crystallizing centres, there has been such mutual interference that
no single individuals liavo been able to assume perfect or even
characteristic forms. The particles in a granular structure differ
much in size. When coarse, the mineral is described as coareely
granular ; when fine, finely granular ; if not distinguishable by
the naked eye, tho structure is termed impalpable. Examples of
the first may be observed is. granular carlionato of lime, of tli»
MINERALOGY
371
■econd In some varieties of specnkr iron, of the last in chalcedony,
opal, and other species.
The above tjrms are indefinite, bnt of necessity, as there is
ev'jry degree of fioeneas of structure in the mineral species, from
perfectly iinpalpable, through all possible shades, to the coarsest
granular. Trie term phanero-crystallino has been used for varieties
in which the grains are distinct, and crypto-crystaUine for those
in which they are not discernible without the aid of a lens.
Granular minerals, when easily crumbled in the fingers, are said to
he friable.
The minute or crypto-crystalline minerals form aggregates some-
what similar to the above. When globular or oolitic, the minute
crystals often appear to radiate from a centre, or form concentric
crusts. These are often globular or nodular; as in dolomite. Some-
what similar are the stalactites and stalagmite^ in which the
mineral (especially rock-salt, calc-spar, malachite, haematite,
limonite) has been deposited from a fluid dropping slowly from
some overhanging body, or some rent in the roof of a cave. In
this case there is generally found a long pendent cylinder or cone,
the principal axis of which, generally hollow, is vertical, whilst
the marginal parts are arranged at right angles to it, except where
they curve round the termination of the tube, when they become
hemispherical.
By far the largest masses of the mineral kingdom have, however,
been produced under conditions in which a free development of their
forms was excluded, and are termed amorphous. This has been the
case with the greater portion of the minerals composing rocks or
filling veins and dykes. The structure of these masses on the large
scale belongs to geology, but some varieties of the textures, visible
in hand specimens, may be noticed. The individual grains or
masses have seldom any regular form, but appear round, long, or
flat, according to circumstances, and as each has been more or less
checked in the process of formation. Even then, however, a certain
regularity in the position of the parts is often observable, as in
graphic granite, where the axes of the skeleton crystals of qnartz
»re parallel. The rock is termed massive when the grains which
form it are small, or granular when they are longer and more dis-
tinct. Sometimes the rock becomes slaty, dividing into thin
plates ; or concretionary, forming roundish masses ; at other times
the interposition of some foreign substance (gas or vapour) has
Tendered it porous, cellular, or vesicular, giving rise to drusy
cavities. These cavities are often empty, but have occasionally
been more or less filled by products of change in the rock. It is
named araygdaloidal when the cavities so filled have the form of
an almond.
Changes of Crystalline Structure.
i " Pseudomorphs " are minerals which appear under a
fqpn of crystallization which does not belong to the
species. They may be recognized either by their having
no cleavage, which is most usual, or by their cleavage
being altogether di£ferent in direction from that of the
mineral imitated. Generally they have rounded angles,
rough and dull surfaces, and when broken show a granular
structure. The faces of the crystal, moreover, are often
covered with minute crystals of a form different from that
of the mineral imitated, but which is that belonging to the
substance now present. Occasionally the resemblance to
real crystals is so perfect, from the perfect polish of the
faces, that they are distinguished with difficulty. They
may be frequently found stiU undergoing change.
Pwndo- Pseudomorphs have been classed under four heads: —
iuor]>hj 1. Pseudomorfha by AUcration. — Formed by a gradual change of
classi- compostion in a species. Of these there are two varieties: they
Sfil. may be pseudomorphous by loss of an ingredient, or by addition of
an ingredient ; change of angite to steatite is an example of the
fii-st, and of galena into anglesite is one of the second.
2. Pseiutoinorpha by Substitulion. —Those formed by the replace-
ment of a mineral which has been removed, or is gradually under-
going ismoval; e.g., galena takes the form of pyromorphite.
3. Pseudomorphs by iTicnistatum.— Those formed through the
incrustation of a crystal, which may be subsequently dissolved away.
Often the cavity is afterwards filled by infiltration; e.g., change of
fiuor to quartz.
i. Pscudomorpha by Paramorphism. — Those formed when a
mineral passes from one dimoi-phous state to another ; e.g., change
of aragonite to cilcite.
' These different kinds of change arc not always distinguishable.
» In some cases a change may take place through alteration of the
anrface, and then, this process ceasing, the interior may be dis-
solved out, leaving a pseudomorph like one of incrustation ; or a
Wendomorph that appears to be a result of mere chemical altera-
tion may be wholly due to sahstitutiou simnly.
Again, changes of scapclite to a felspar, and of augite to nralite
(hornblende), have been considered by Scheerer examples of
paramorphism, — scapolite being considered dimorphous with some
felspars, and augite with hornblende. But, while such paramorphic
changes undoubtedly take place with aragonite, their occurrence in
these silicates — which are common associates in the same rock, and
must have been formed under like circumstances — is hardly prob-
able.
Where mineral bodies have taken the form of organisms, it id
more a case of molecular replacement than of true pseudomorphism.
Pseudomorphism should be understood, however, to consist, not
simply in alteration of crystals, but in many instajices of changes
in beds of rock. Thus all serpentine, whether in mountain masses
or in simple crystals, has been formed through a process of pseudo-
morphism— or, iu more general language, of metamorphism — of
olivine and augite. The same is tnie of other matrnesian rocks, aa
steatitic, talcose, and chlorite slates. The crj'stalline rocks often
offer examples of a change similar in nature. The graphite of these
rocks is probably but a metamorph of some vegetable organism.
Thus the subject of metamorphism, as it bears on all crjstalline
rocks, and that of pseudomorphism, are but branches of one system
of phenomena ; the chemistry of both is the same, and a knowledge
of such changes is indispensable to a study of the older rock strata
of the earth.
The common change of pyrites, forming the laain ingredient of
the upper part of metallic lodes, to earthy red or brown iron ore,
thus producing the "gossan" of miners, is one of many examples
of these processes now in progress. Often the gossan contains dis-
seminated silver or gold, derived from the decomposed ores. This
is a case of pseudomorphism, as truly as when a simple crystal of
pjTites becomes limonite ; the mode of change and its laws are
the same. Again, phosphates,
vanadiates, and arseniates
of lead, &c., as well as car-
bonates and sulphates, are
among the surface species,
or those that occupy the
npper part of metallic lodes ;
they are the results of altera-
tion within those depths to
which atmospheric agencies
penetrate.
Pseudomorphs are always
records of past existences, in
some cases they may be the
only evidence we possess of
such prior existence. Tigs.
238, 239 are pseudomorphs
of quartz or homstone after
datholite ; the measured
angles of these crystals show
that the imitated crystal was
datholite ; but that mineral
does not now occur in crystals
of either of these forms.
Tho process of petrification
of organic bodies is in realitj'
a species of pscudomorphic
formation, and has been pro-
duced in all the above modes.
External and internal caste of organic bodies are not uncom-
mon. In other cases the original substance has been replaced
by some mineral which has preserved, not merely the external
form, but even the minutest detail of internal structure,— so that
the different kinds of wood have been distinguished in their silici-
fied trunks. The most common petrifying substances are silica
and carbonate of lime. In encrinites, echinites, balemnites, and
other fossils, the crystals of calc-spar often occur in veiy regular
positions. In some varieties of petrified wood both the ligneous
structure and the cleavage of the calc-spar are observable.
Different from the above are mineralized bodies, in which the
original structure is still retained, but their chemical nature
partially changed. In these a complete series may be often traced,
as from wood or peat, through the varieties of brown coal,
common coal, anthracite, and graphite.
Cav3es of Change.— The causes of change are the Origin o«
simplest and most universal operations about us : — (1) the P^^™j^
process of gradual alteration to which some substances are ^
liable on account of the presence of oxygen and carbonic
acid in the atmosphere, and the reaction of substances thus
formed on adjacent ingredients, aided or promoted by
electrical currents or by heat; (2) the solvent power of
ordinary waters, cold or hot, or of steam ; (3) reactions,
in accordance with chemical principles, of the ingredients
Fig. 239.
372
MINERALOGY
dissolved in these waters, or in mineral or sea waters, Lejited
or at the ordinary temperature ; (4) the action of gases ex-
haling from the earth ; (5) changes referable to volcanic
action.
Ordinary waters hold in solution, as is well known, more or less
,of mineral matter. AVlicn water containing carbonic acid is passed
throagh a large number of ordinarily occurring miuerals, it gives
evidence of the presence of au alkali, or lime, or magnesia; and
some of these minerals give tho tests even with the first drops.
Pure water gives with many of them a similar result, but more
slowly. Limestone in forty-eight hours yields soluble ingredients
^to the extent of 0*4 to 1 per cent, of the whole mass. The lime,
magnesia, and alkalies appear in the condition of carbonates ; and
the iron passes from the state of carbonate- to that of peroxide
iduring evaporation. The silicates of magnesia, lime, and man-
ganese are especially ready in yielding to this action. Silica,
however, is more soluble in ordinary than in carbonated water.
)L These facta illustrate two important points; — (1) that ordinary
, waters lying upon ond filtering through the earth's crust are
constantly active in dissolving and decomposing minerals and
rocks, and that even species reputed indestructible are thus acted
upon ; and (2) that the waters are thus furnishing themselves with
agents capable of effecting other chemical changes. These waters
penetrate all rocks, as well as percolate through soils. Hence the
action is a universal one, everywhere going on ; and the results are
universaL Bones, shells, corals, and animal remains generaDy
are also sources of carbonate of lime, phosphates, and nuorides ;
iind plants may contribute also potash and soda, and sometimes
eUica. _
Carbonic acid is a constant ingredient of the atmosphere, and is
dissolved by the ri\ins as they descend ; hence this active de-
composing agent is present in ail ordinary waters; but it is also
a result of ditTerent mineral changes. Sulphate of iron ^long
with vegetable matters gives oxygen to the carbon of the vegetable
matter, and thus produces carbonic acid and pyrites or sulphuret
of iron ; and the large quantities of pyrites in coal-beds show on
how grand a scale this process has taken place. Sulphate of zinc
in a .similar manner produces carbonic acid and blende or sulphuret
of zinc, Bischof observes that the carbonic acid which has thus
been eliminated must have been sufficient in quantity to make an
atmosphere of carbonic acid equal in height to our present atmo-
sphere. Again, decomposition of sulphurets produces sulphuretted
hydrogen ; this by the oxidating action of the atmosphere forms
sulphuric acid, and the sdlphuric acid acting on Hmestoue produdes
gypsum, and liberates carbonic acid. Sulphurous acid is also
generated in the neighbourhood of volcanoes, and rapidly becomes
sulphuric acid, with the same result. Moreover, silica in waters, if
aided by heat, will decompose limestone and liberate carbonic acid.
Hence it is that this gas is exceedingly common in exhalations from
mineral springs ; indeed it occurs more or less iu all watera.
The dissolving and decomposing action of carbonated waters is
therefore general. The sea also partakes of this character, and, iu
Tirtue of the numerous salts whicn it holds dissolved, is a powerful
agent in carrying on the changes to p-hich the process leads. Such
changes -ajid the various pseuaomorphs to which they give rise have
to be regarded as types and evidences of vast metamorphic transfor-
mations,— processes either of decav or of reformation which have
modified widespread rock-masses, and which are at the present
time altering the structure of the crust of the earth. It is tnrough
a study of pseudoraorphs, and of the processes which have gone to
form thera, that mineralogy is to become the germ from which
alono the petrological department of geology can have its true
development, and become a living instead of a merely speculative
science.
Physical Propeetie3 of Minerals.
Characffrs Dfjyfndiny on Light,
. Theie are few more interesting departments of science
than the relations of mineral bodies to light, and the modi-
fications which it undergoes either when piassing through
them or when reflected from their surface. In this place,
however^ wo only noticG these phenomena so far as they
l>oint out distinctions in the internal constitution of miuerals,
or furnish characters for distinguishing one species from
another.
Lusrw of Zw5?rf.— Though tho varieties of lustre admit of no precise
mtQcrals. gr mathematical determination, they are of considerable
value in mineralogy. One highly important distrnction
founded on them is that h)etween minerals of metallic and
non-metallic aspect or character. Transparency and opacity
nearly coincide with this division, — the metallic minerals
beinf: almny.t constantly opaque, the non-metallic more or
less transparent. Minerals which are perfectly opaque,
and show the peculiar brilliancy and opacity of surface of
polished metals, are named metallic ; those which possess
the.se properties in an inferior degree are semi-metallic;
and those "without these firoperties arc non-meta.Uic.
Lustre has reference to cither tho I'ntensity or tfie quauty of the
reflected light, considered as distinct from colour. Several degrees
in intensity have been named:— (1) splendent, when a miiiiTal
reflects light so perfectly as to be visible at a great distance, ai)d
lively and well-defined images are fomied in its faces, as galenn,
specular iron, or cassiterite ; (2) shining, when the reflected light
is weak, and only forms indistinct and cloudy images, as heavy
spar or calcito ; (3) glistening, when the reflected light is so ftcblo
as not to be observable at a greater distance than arm's luicth, ajid
no longer forms an image, as talc; (4) glimmering, wncji the
mineral held near the eye in full clear daylight presents only a
number of small shining points, as red b.cmatite und granular
limestone. When, as iu chalk or kaolin, the lustre is so feeble as to
be indiscernible, the mineral is said to be dull.
In regaid to the kind or quality -of the lustre, the following
varieties are distinguished :—{l) the metallic, seen in much per-
fection in native metals and their compounds with sulphur, and
imperfectly iu glance coat; (2) adamantine, found in beautiful pei^
fection iu the diamond, aud in some varieties of blende anjl
cerussite ; a modification is metallic adamantine, a^9 seen in wolfr^n
and black cerussite ; (S) vitreOus or glassy, seen in rock crystal, or
common glass, or, inclining to adamantine, in flint glass ; sub-
vitreous is seen in broken caJcite ; (4) resinous, when the body
appears as if smeared with oil, as iu pitchstone, blende, and
garnet ; (5) waxy, like beeswax, as seen in wax-opal and ozocerite ;
(6) pearly, like mother-of-pearl, seen in gyrolite, talc, heulandite ;
(7) silky, the glimmering lustre seen on fine fibrous aggregates like
amianthus, tremolite, chrysotile, krokidolite.
These degrees aud kinds of lustre are generally exhibited differ-
ently by unlike faces of the same crystal, but always similariy by
like faces. The lateral faces of a right square prism may thus
difl"er in lustre from that of a terminal face. Thus the lustre of tho
lateral faces of apophyllite is vitreous, while that- of the terminal,
at right angles thereto, is pearly ; chrysotile is silky when split
along the fibres, dull when at rig'ht angles to them.
The surface of a cleavage plane, in foliated minerals, generiiiij
differs in lustre from the sides ; and here again in some cases the
latter are vitreous, while the former is pearly, as in heulandite.
As shown by Haidinger, only the vitreotfs, adamantine, ind
metallic lustres belong to faces perfectly smooth and pure. In the
fii-st, the index of refraction of the mineral is 1'.3 to I'S; in tho
second, 1 9 to 25 ; in the third, above 2"5. The pearly lustre is a
result of reflexion from numberless lamellce, or cleavage planes,
within a translucent mineral; and in hydrated minerals, as in thtf
zeolites, it is the result of incipient change, — namely, a loss of water
which ensuea upon exposure to the ahnosphere.
Colour. — This \s a property wfiicb is ot very inferior Colow.
value. Minerals are so seldom, if ever, absolutely pure
that very minute quantities of an intensely coloured
impurity may imimrt colour to a substance inherently
colourless, or overpower a feebler colour which may be
its own.
Some few minerals have colour so strong, or have a constitution
so little susceptible of intermixture, tdat thoy retain almost unim-
paired the colour sjiccial to theni. Such a substance is pyritc ; its
brass-yellow colour may be heightened to cold-yellow by intermixture
with copper sulphide, or it may be slightly Ij'ci^^hcd by ai-senic ; but
the nature of its composition tloos not adndt of the intrusion of oidl-
naiy colouring iiigicdients. The yellow of native goM, again, maybe
l>aled by impoverishment ^ith the white of mIvut, down to the dull'
tint of elcctrum ; but no fort-ign colouring matter can intrude itself
into a metallic mass. Such bnl>stanccs as thcsr,— native uu-tals/
sulphidca, and oxides, — have coloui-s essential to them, dci)cndeiit
on thoir constitution, and to a gicat extent cha>-actctistic of tho
species.
A second class of minerals are colourless of themselves, and thus
very subject to the influence of minute quantities of foreign tiuc- '
torial impuritj'. These aio absolutcl}' transparent and devoid of
colour wncn in crystals, but white and opa<ino when reduced tD
powder ; as ice and snow, calcito and cliaik, rock-crystal and
sand. But surh substances arc geneially coloured ; " muddied " it
would bo called in the first case, though it in equally so with tho
othci-s. Such false colour may be inniartcd in several ways. It
may be (1) fi'oni their liolding dissolveJ some colouring matter ; (U)
from mechanical mixture of colouring substances such as metallic
o.NJdes, or minute crystals ( " cndoraorphs ") o/another mineral; or
MINERALOGY
573
/S) from chemical replacement, — the substitution of a smaller or j
larger quantity of a coloured isomorphous ingrcdieut.
As illustration of the first, silica, colourless in rock-crystal, has
heen fo\uid of almost every tint, due frequently to volatile hydrocar-
bons which are dissipated by heat. Fluorite also, found of almost I
every shade of every colour, may possibly bo to a certain extent
referred here. ' -
Quartz, felspar, and calcite are often coloured accidentally by
imbedded layers of foreign "inclusions," or by " spangling endo-
tnorphs." These arc mechanically mixed, so far as regards their
prcsenci) in a structure of different and nonassimilable chemical
comiiosition, but crystallographically arranged. They either mark
the lines of interrupted or intermittent giowth; or, in the case of
endomonihs, the axial positions of the minute intniding foreign
rrystals lie in one plane, or in the same sets of planes.
1^ As an instance of colours introduced through definite chemical
axidaccraent, calcite may be cited. Carbonate of lime is colourless ;
if a portion of this be replaced by carbonate of magnesia there is a
^rtain amount of pearly opacity ; if by carbonate of manganese,
of a pink tinge ; if by carbonate of iron, of yellow, which may be
increased through oxygen absori»tion and " weathering " to an ochre
tint, and ultimately to a dark brown.
Sulphurct of zinc, chemically white, and mincralogically trans-
parent, may, through metallic substitution, be found of almost all
tiuts of yellow, orange, brown, and black. Again, hornblende,
ftugite, and garnet,— silicates, wliich in their purest states of tremo-
lite, malacolite, and water garnet arc colourless, — acquire green,
b^o^vn, red, and black tints from the assimilation of other metallic
•ilicites.
I Hence it would appear that a very advanced practical know-
ledge of the subject is necessary to enable us to avail ourselves
«f the information which is to be derived from this external
feature.
The accidentally coloured minerals sometimes present two or
more colours or tints, even in a single crystal, — very remarkable
examples occurring in iluor-spar, ajiatite, sapphire, amethyst, tour-
maline, and cvauite. This is stilt more common in compound
Diinerals, on which the colours are variously an*angcd in points,
streaks, clouds, veins, striiios, bauds, or in brecciated and ruin-liko
forms. Some minerals again change their colour from cxjK>suro to
light, the air, or danj[>. Then either the surface alone is affected
or "tarnished," and appears covered as with a thin film, producing
in some minerals, as silver and arsenic, Duly one colour ; in
others, as chalcoi>yritc, hnsmatitc, bismuth, stibine, and anthracite,
.vario\is or iridescent hues, wlicn they are said to have a
•pavonine lustre. Or occasionally the change pervades the whole
mineral, the- colour either becoming paler, or disappearing, as in
chrysopraso and rose-quartz, or becoming darker, as in brown
Bpar, siderite, and rho<louite. In a few minerals a complete change
pf colour takes pl.TCe, .is in heterosite, and in the chlorophtcito of
^ho Western Isles of Scotland, whidi, on exposure for a few hours,
Iklsscs from a transparent yellow-green to black. Tliese mutations
«re generally connected with some chemical or physical change,
trhe tarnished colours sometimes only appear on certain faces of a
Irrystal belonging to a peculiar form. Thus a crystal of copper
liyrites (like tig. 89) has olio face F free from tarnisli ; the faces b
bnd c, close to F, dark blue; the remainder off, first violet, and
llien, close to P, gold-yellow.
^ Some crystalline minerals exhioii in certain directions a very
lively play or change of colours from reflected light. It is well seen
in many various hues on the cleavage-planes of labradorite^ and
sei-ms produced by a multitude of very thin quadrangular pores,
interposed in the mineral, like minute parallel laminrc. On the
cleavage-planes of hyiiersthcne ^ it appears coiiper-rcd, and is
occasioned by similar iwres, or by iiunicrous small brown or black
laroiiix of some foreign substance interiHxsed in a itaiallel ix>sition
between the planes of the hyiier^thene. The cliatoyant or changing
colours of tliu sun-stone arise from scales of Ineniatite similarly intor-
|ioscd, and that of av.nnturiiie from scales of mica. The play of
colour in the noble oi>al scciiis lo be producvd very neatly in the same
manner as that in the labradoritc. A similar oi<ilesccncc is seen
ill certain minerals when cut in )>articular forms. In the saiqdiire,
ctlt hemispherically over the chief axis, it appears like a star with
six rays; in garnet it shows four rays; in certain varieties of chryso-
b«ryl andofadnlaria it has a bluish lint: and it is also very remark-
able in the cal's-eyo variety of quartz. Iridescence often arises from
very fine fissures, producing semicircular arches of prismatic tint.s,
which, like the colours of thin plates in general, arc i-cferred to the
iulcrfercncc of light.
Jtreak. Streak. — Tbis name is applied to the ajijiearance and
the colbur of the line or furrow produced in minerals by
drawing the edge of a hard-tempered knife or file along
their surface, or to the stain obtained by rubbing a soft
mineral on such a substance as paper or )>orcelaln. Taken
along \vith the hardnebs, which may to a certain extent be
determined by the same operation, it is one of the most
valuable tests which we possess.
The furrow may be lustrous or it may bo dull. '•' Powder of
splinters may lie along its course, or a still adherent ridge may havo
been merely rolled over. The fuiTow and the powder may each bo
possessed of colour, though* such may not be distinguishable in the
mineral, or may havo a colour quite diflercnt from that of the
mineral. Three illustrations of tnc usefulness of this test may
suffice. Argentiferous gold, chalcopyrite, and pyiitc, diflering
immensely in value, may readily oe mistaken for each other.
The knife, when drawn along the surface of the first, sticks in it,
ruts up an adhering ridge, and leaves a shining streak of the same
colour as the specimen. When drawn along tlie second it ruts up
a trench covered with a dusty powder, which when rubbed on paper
or in the hand is greenish yellow. \Vlien diawn along the third
it has no effect, as pyrite is harder than the knife. I'silomclane,
haematite, and limonite all occur in black, glossy, stalactitic fomu^
and have all been termed '* black hiematitc." There is here also
great difference in the value. The knife makes little impression on
psilomelane, but leaves a blue lustrous line ; it makes a blood-rcd
line in htematite, and a rich ochre-ycllow in limonite. Gra|>liit«
and molybdenite both crystallize in hcxaOTUal plates, both occur in
the same rocks, both have a grey-black colour and a brilliant
metallic lustre, both stain the hands or j-apcr ; the streak of tho
first — best seen on paper — is black, tending to blue ; that of the last
is greenish. Rough porcelain is the best material for deteiTOining
the streak of soft minerals.
Diaphaneity. — Jlinerab, and even different specimens of Tram-
the same species, vary much in this quality. Some nnssion,
transmit so much light that small objects can be clearly^"**'''
seen, or letters read, when placed behind them ; such are
named transparent. They are seniitransparent wjien the
object is seen only dimly, as through a cloud, and translu-'
cent when the light that passes through is so broken that
the form of the object can be no longer 'discerned ; some
minerals are only thus translucent on the thinnest edges.
Others transmit no light, and are named opaque.
Refraction. — It has already been mentioned that most Boubia
crystals — all, in fact, except those of the cubical system— rcfrac,
ejdiibit the phenomena of double refraction. For a •
general explanation of these phenomena the reader is
referred to Light, vol. xv. p. 609 sq.
The direction in which there is no double refraction is named Opti^
the optic axis of the crystal, — sometimes, less happily, the axis of ax;s,
double refraction. Now in certain minerals it is found that there''
is only one (Urection with this property, whereas in othcnj there
are two such directions ; and they have in ronsei|Uence b^en divided
into nninxnl and biuaxal. To the former belong all crystals of
the tetragonal and hexagonal systems, to the latter all those of the
other thi«e systems. In the foimer the optic axis coincides with
or is parallel to the crystallographic diief axis. In some uniax.il
crystals the index of refraction for the extradnliiiary ray is great-T
than for the ordinary ray ; and in otheis it is smaller. Accordiug
as it is greater or less they are said to have iiositive (atti^ctive) or
negative (repulsive) double refraction. f- ■\ )
(Juartz is an example of the former, the index of refraction, accbnl-
ing to Malus, being for 0-1-5484, for E- l-5!;82; calc-spar of tlio
latter, the index of O being -1-6543, that of E 14833. The
index of E is in both cases takeu at its maximum. - ,
It should be observed that the optic axes arc not single lines, bnt
directions parallel td a line, passing through every jvirt of tho
crystal. It is also important to remark that this proiicrtv divides
crystals into three precise groups : — the cubic, with singly refrac-
tion ; the tetragonal and hexagonal, w-ith double refraction, and
uniaxal ; those of the other three systems, also double, but binaxal.*;
These jiroix-rties are therefore of the (.Tcatest use in detei-miniag'
the system to wliich a mineral belong.
Polarization. — Intimately connected with this i>ropcrty Pol,tri'a'
is that of the i>olarization of light, which affords an easier •""-
means of determining mineralogical characteristics than
the direct study of double refraction. For the elements
of this subject see Light, vol. xv. p. 611 e-j.
AVhile a consideration of the optic axes enabled us
merely to arrange the systems of crystallization in thred
groups, the phenomena of jiolarization not only bear out
a furtlier subdivision of the whole into the above ail
systems, but disclose, in many cases, phenomena markedly
special to individual species. The optical consideration
of these ijhenomena enables us to fix three directions Jit
'374
MINERALOGY
Axfs of rignt angles to one another — called tlie axes of optical j
optical elasticity — such that the effect of the crystal on the '
*}^^'" luminous vibrations of the elastic ether is a maxiraiun in
' one of these directions, a minimum in "a second, and a
maximum-minimum iu the third. The length of these
axes is chosen in terms of this action. In certain cases
the direction of the axes of optical elasticity is different
for light of diffe 'ent colours.
The position of these axes in relation to the crystalloCTaphicaxes,
and tho ratios of their lengths, enahlo ua to class all crystals aa
follows: —
1. Crystals of the cubic system. Here the three axes of
elasticity are all equal. The refraction is siiuplo.
2. Crystals of the tetragonal and of the rhombohedral systems.
Two of the axes of optical elasticity are equal iij these systems ; the
third is greater or less according as the crystals are negative op
positive. Tho t^o equal axes lie in a plane perpeudicular to tho
principal crystallograuhic axes ; the third axis ooincides with the
principal axis.
3. Crystals of tho right prismatic system. Tlio direction of the
three axes of optical elasticity coincides with the crystallogiaphic
axes, taken parallel to the diagonals of the base of the rhombo-
hedron, and to the vertical edge of the prism (the primitive parallel-
epiped of Levy).
4. Crystals of the oblique prismatic system. Only one of tho
axes of optical elasticity coincides necessarily with the crystallo-
graphical horizontal axis, or the diagonally horizontal axis of tliQ
rhombic base, the direction of the j two others not having any
evident relation, a pnori, with the inclined or diagonally inclined
axis of the base, and with tho vertical axis (or verticsd edge of
the primitive parallelepiped).
5. Crystals of the anorthic system. The three axes of optical
elasticity have no relation that can be assigned a priori to the
crystal! ographic axes, whatever position may be assigned to these
in relation to the primitive solid
In crystals belonging to the last three systems the three axes of
elasticity are unequal.
Tho axes of elasticity are in general such that a ray passing
through tho crystal in the direction of any one of them is divided
into two, which follow that direction with different velocities
depending on the lengths of the other two axes. To iny other
direction there will in general also correspond two difTorent
velocities ; but their ratio will now depend in a more complex
manner on all three axes. In two directions (and only in two, if
the axes are all unequal) the ratio becomes unity, or the ray is not
divided. These directions are the optic axes.
The displacement of the axes of elasticity for light of different
colours, already mentioned, takes place for two axes in crystals of
the oblique prismatic system and for all tliree axes in tho anorthic
{i.e., doubly oblique) system. In tho other systems it does not
occur.
Colour In order to follow the distinctive features of the different systems
pheno- farther, it is necessary to consider the ci^our phenomena which
jnena, they display, when examined in a beam of polarized light. Vari-
ous instruments have been devised for this pui'posc, as, e.g., the
polarizing apparatus of
Norreiiberg, htted with
a condensing lens below
and above the crystal
slice, or with a low-
. power (3-incli) eye-piece.
The polarisGope of Hoft'-
man of Paris is more
efficient, but the apja-
fatus of Deacloizeaux
(fi^. 240}, who has made
this modo of irivestiga-
tion a special study, lias
the widest scope of use-
fulness. In this appa-
ratus a blackened mirror
is employed for polariz-
ing tho light, taking tho
place of a tourmaline
plate, a Nicol's prism,
or a bundle of thin glass.
The mirror is inferior
to tho other two in completeness of polarizing power, and in not
admitting of rotation ; while it shares tliis defect with tho last.
It in, however, Huperior to all in extent of field,
not, liko tho tirat, alTect whili> light. A Nicol's pr
examining or analysing the light which passes.
The descrintion of the many beautiful phenomena that may bo
observed witri polarizing apparatus when applied to sections of
crystals belongs to the subject of Optics (Puysical), to which
Via. 240. — Apparatus of Descloizeaux.
ivhilo it d(
J used for
.^'"W^
heading also we rjr.st refer for the phcuumOTa of circular
polaiization.
Double Jiefraclion and Polarization of Composue Crystals.— h. •'t''--
all tho crystallized bodies whoso action upon light we have beei. l^rope^
considering, tlie phenomena are identical m all parallel directions, ''-ea of
the smallest fragment having the same property as the largest, compoiite
from whatever part of tho crystal it is taken. In the mineral cryatala.
world, however (and among tho products of artificial crj'stalliza-
tion), there occur crystals which are composed of several individual
crystals whose axes are not parallel. These crystals sometimes
occur in such regular symmetrical forms that mineralogists have
long regarded them as simple forms ; and it is probable that they
would have still been so viewed if they
had not been exposed to the scrutiny of
polarized light.
A composite structure has been on
served in the case of Brazilian topa/,
sulphate of potash, and apophyliitr
Bipyramidal sulphate of potash, whi' '
Count Boui'non supposed to be a siiiiil
crystal, was found to be a tesselat^l
crystal, composed of three pairs of crystal
of the prismatic sulphate of potash coin
bined so that each pair had their principal
axes parallel. When exposed to polarized
light, each pair gave the system of biuaxal
rings, and when held at a distance from
the eye had the tesselated appearance shown in fig. 241, each
opposite pai'" of the triangles having the same tint.
The most remarkable of this class of minerals is the tesselated
apophyllite. The examination of this body by polarized light is
duo to Brewster. For his results the reader is referred to his paper
in tho Edinburgh Transactions, vol. ix. p. 323.
Figs, 242, 243 are representations of the figure produced in-
polarized light by an internal slice of the barrel or cylindrical
Fig. 241.
Fig. 242. Fig. 243.
apophyllite from Kudlisaet, m Diaco Islana. The figiires are from
different specimens. The shaded part of them has only one axis
of double refraction, while the foiu- sectors have two axes. The
mechanical structure of the cleav-
age planes resembles the optical
figure even after the planes are
ground.
Tho minerals stilbite, heuian-
tlite, chabasito, and many others,
arc similarly complex in struc-
ture.
Crystals with Planes of Double
Refraction. — Analcime, a mineral
ranked among tho cubical crys-
tals, was found by Brewster to bo
singular in its action upon light,
and to exliibit tho extraordinary
ju-operty of many planes of double
refraction, or planes to which the
double-refracting structure was related in the same manner as it is
to one or two axes in other minerals. It crystallizes most com-
monly in tho form of the icositetrahedron. If wo suppose a com-
plete crystal of it to bo exposed to polniizod light, it wdl give the
remarkable figvire shown m fig. 244, where the dark shaded lines
represent planes iu wliich there is neither
double refraction nor polarization, — the
double refraction and tho tints commcnoin^
at thcso planes, and reaching their maxitnutn
in tho centre of the smce enclosed by three
of tiio dark lines. Wlieu light is trans-
mitted through any pair of the four planes
which are adjacent to any of the three axes
of the solid, it is doubly refracted, the least
refracted image being tho extraordinary one,
and consequently the double refraction nega-
tive in relation to the axes to which the doubly-refracted ray is
perpendicular. If we suppose the crystal to have the form of A
Fig. 244.
Fjg. ::4i
MINERALOGY
375
eotw, :h- p'uu of doabla rafnctioa will be, u in fig. 24S, t
pliin< ;~--'-V chroogfa tl» two diagonals of aach tact of the cub*.
The'tioti Tary a* the iqiiate of the Hiit»nim from tli< neanat plana
of double rafnictioD.
rifiKKroim. — Closely connected with double refraction
ia that property of transparent minerals named pleochroism
(of many colour!)), in consequence of which they exhibit dis-
tinct colours when viewed by transmitted light in different
directions. Crystals of the cubic system do not show
this property, whilst in those of the other systems it
appears in more or less perfection, — in tetragonal and
hexagonal minerals as dichroism (two colours), in the
rhombic and clinic systems as trichiroism (three colours).
lo most cases these changes of colour are not very decided,
and appear rather as different tints or shades than as
distinct colours. The most remarkable of dichromatic
minerals are the magnesian mica from Vesuvius, the tour-
maline, and ripidolite ; of trichromatic, iolite, andalusite
from Brazil, diaspora from Scbemnitz, and axinite.
In a specimen of yellow Iceland rpor the extratTrdinary image ia
of an orange. yoUow colour, while the ordinary image is yellowish
white. AloDg the axis of double refraction the colour of the two
pencils is exactly the same, and the difference of colour increases
with the inclination of the refracted ray to the axis. This is
the invariable law of the phenomena in nniaial crystals. Sir
John Hcrschol found several (ourmalinea to have a blood-red
colour along the axis, and at right angles to it to be yellow -green.
Then can bo little doubC that this property will bo found in every
crystal of sul&cient retraction. Even if the crystal is colourless,
• slight inequality in the intensitv of the two images may be
oSeervcd ; and when it is distinctly coloured the diSerence of
intoDiiity is very easily seen, even when the two colours are not of
a ditfcruat kind.
The phenomena of dichroism are best seen in crystals with two
axes of double refraction, and are well exemplified in iolite, a
mineral which crystallizes in six- or twelve-aided prisms. These
prisms are of a deep blue colour when seen along the axis, and of
a yellowish brown colour when viewed in a direction perpendicular
to it
If nbi^ (fig. 148) is a section of the prism of iolite in a plane
parallel to the axis of the urism, the ti-aosmitted light will be blue
through the faces ab and ac, and yellowish brown
through ad, 6c, and in every direction perpendicu-
lar to the axi^ of the prism. If we grind down
the angles a, c, A, (i, ao as to replace them with
faces iMH, ni'n' and op, </p', inclined 31' 41' to ad,
or to the axis of tlie prism, then, if the plane
»ied passes through the optic axes, ne shall
obaerve, by trausmittiug polari2e<l light through .i\ /''
the crystal in the directions ac, bd, and aubae- » «'^
^nentty analyaiu^ it, a aystem of rings round ooch *"'g- 24*.
of three a-tes. The syitom will exhibit the individual rings very
plainly if the crystal is thin ; but if it Is thick, we shall observe,
when the plane ahai is perpendicular to the plane of primitive
polarization, some branches of
blue and white light diverging
in the form of across from the
cootiT of the system of rings,
or the potoi of no [polarization,
as shotrn at /' and p (fig. 247),
whoro the shaded branches
irprrscnt the blue ones. The
summits of the bluo masses
an) tipfii.Hl with purple, and
nn.' ». Ml itod by n'hitish light
ill ■{ccimons and vellow-
i.' Ill othcre. The white
li^li*. 1 ■:■ oinos more hlue from
^o and // to o, where it is quito
blur, and more yellow from p
and p' lo c anil >/, where it is
roni|.I.t>lyj-cllow. Wicn the
phiii- '('.-.( 13 in the plane of primitive polarization, the poles p, ^
art niiik«l by s]iots of whits light, but everywhere else the light
is a -I'-cp bluo.
Ill tlio plane atHb (fig. 247) the mineral, when we look through
dt by common light, exhibits no other colour but yellow, mixed
with a small iiiiaiitity of blue, polarizeil in ai>opiwsitr pisne. The
•nlinarv image at cand rf is yellowish brown, and the extraordinary
image faint blue, the former receiving aorae blue ravs and the
latter some yellow ones from candifton and 6, whore the ditlorenco
,«f colour is still wrll-markod. The yellow image becomes fainter
tnm a and i to p and/, till it chaugea into blue, and the faint blue
r
im«g« ia itrcngthened by other blue nyn, tiD the intensity ofthe two
blue inugn ia nearly er|aal. As the incident rmy adTUc«s fVoro o
and<itopand/f', the faint bine image becomea more intenae, and tho
yellow one. receinng an acceaaion of blue raya, becomes of a bloiah
white colour. The ordinary imafra ia wbituh from p and j/ to o^
and the oxtraordinary ia aeep blue ; but the whtteneaa gTadually
diminiahea towarda o, when they are both almoat equally blue.
The principal axis of double refraction in iolif'c ia negative. The
moat refracted imaga ia ourpUah blue, and the Icaat refracted ono
yellowish brown.
Brewster found that the dichroism of aereral crystals ia changed
by heat, and that in some coses this property may bo commnni-
catiMl to them. Babinet foand that all negative cryatals, such us
calcorvoua spar, corundum (including ruby and sapphire), tour-
maline, and emerald, absorb in a greater degree the ordinary ray,
with the exception of beryl, apatite, and some apophyllites ; wbila
poaitive crystals, such aa zircon, smoky quarti, sulphate of limu,
and common apophylUte, absorb in a greater degree the cxtroonli-
nary ray- Babinet foujd also that certain crystals, such as red
tourmaline and ruby, transmit nya of their peculiar colour without
being polarized, — in which caaea the black croaa of their system of
riof^ IS coloured, and this nnpolarixad light exists both in th«
ordinary and extraordinary ray.
Hiiiduigor devised an instrument for showing ana for testing tha
pleochroism of minerals. In fif. 248, p is an oblong cleavage-
rhombohedron of Iceland spar which has two glass priama v,w of
Fia 24S.— Section of Dichroiscopa.
18* cemented to its ends with Canada balsam. This combination
ia placed in a motallio case, which has a convex lens / at ono end
and a square hole o about the fifteenth of on inch in width at tho
other. The lens is of a focal distance which shows an object held
about half an inch from the square hole.
On looking through the lens and priama two imagea of the aqnars
hols are seen just toucliing each other. The Tight of tho one
image is notarized in the plane which intersects the short diagonal
ofthe prism ; that of the other is polarized in the plane of tho
longer diagonal. When a pleochroic crystal or fragment is held at
focal distance and examined by transmitted light, then, on tha'
turning of the instrument bringing the polarization of its planes into
coincidence with those of the crystal, the two iniagea of tho aqoars
opening will show the coloura of the oppositely polarizod pencila of
which tho light transmitted by tho crystal is compoaed; this
conatitutea its pleochroism. The dichroism is then seen by looking
through tho crystal in one direction only, and the contrast of tho
two coloun ia made more obvioua.
Phosphortacfnct. — This is the property possessed by par- Phospfaoi)
ticular nunerals of emitting light in certain circumstancer.
without combustion or ignition.
Thus some minerals appear liuninoua when taken into tho dark,'^
after being for a time exposed to the sun's rays or even to the ordi-
nary daylight. Many diamonds, and also calcined barytas, exhibit^
this property in a remarkable degree ; less so aragotrito, calcsrar,'
and chalk. Many minerals, incmding tho giTator part cf thoao
thus rendered phosphorescent by the influence of the ttun, also
become so through heat Thua some topazes, diamonds, and varie-
ties of fluor-spar become luminous by tho heat of tlie hand ; other
varietit's of tliior-spar, and jphosphoiito, require a teraperatufo near
that of boiling water ; whilst calc-spar and mahy silicates arc only
ph4Wphorc!k-ent at from 400* to 700* Fahr.
imectrictty produces phosphorescence in some minerals, ** i'*
green tluor-spar and calcined DarytcK In othcra it ia excited whra
thoy aro stiiick, rubbed, split, or broken ; as in many varietioa uf
zinc-blende and dolomite when scratched with a quill, pieces of
quartz when rubbed on each other, and plates of mica or needles of
peotoUto when suddenly separated.
The light emitted by phosphorescent minerals is of v^ous tinto,!
Tho variety of fluor called chlorophano emits, as its name oxpreeses;
a green light Tlio aame particle mav emit varying tint.s as in tho
fluor from Aberdeenahire, which, as tlio heat falls, or the onerpy of
tho phosphorescence wanes, emits tints wliich pass from nolot,
through oluo, green, and yellow, to dull purplish red. The yellow
blonde from the same place ia vividly phosphorescent when heatsiT.
Fluor generally phoapboroscea with a tint of its o^ni colour.
Too nigh a beat destroya tho pLoaphorcacence, which may, hpW-
.arsTf^bo rsstond by either exposure to aun'a light or to elsctridty-
676
MINERALOGY
Fhior-
esoence
Electric
proper-
ties of
mneral:
«leetri-
citj-
Whe mineral pnosphorescea viTidly when the dischar^ passes
feiroagh it ; it generally nhosphorescea with, a different colour after
It has been thus recharged.
Fluorescence is the property whereby rays of light of a
refrangibility higher than those ordinarily seen by the
human eye are rendered visible. The substance when
placed in the violet end of the speptnun, and carried be-
yond it into the in\isible rays, becomes luminous, through
"degrading" the rays of extreme refrangibility. This
j)roperty is well marked in those varieties of fluorite which
are pale green by transmitted light, and deep purple by
reflected light. Ozocerite and some petroleums also ex-
hibit the property.
Electric^ Magnetic, and Thermic Properties.
Electricity. — Friction, pressure, and heat may all excite
electricity in minerals. To observe this property delicate
electroscopes are required, formed of a light needle iermin-
ating at both ends in small balls, and suspended horizon-
tally on a steel pivot by an agate cup. Such an instrument,
can be electrified negatively by touching it with a stick of
lealing-wax excited by rubbing, or positively by merely
bringing the wax so near as to attract the needle. When
the instrument is in this state, the mineral, if also rendered
electric by heat or friction, will attract or repel the needle
according as it has acquired electricity of an opposite or of
I a similar kind; but if the mineral is not electric it will
attract the needle in both conditions alike.
Most precious stones become electric from friction, and are either
positive or negative according as their surface is smooth or rough.
Ail gems become positive when polished ; the diamond even when
unpolished is positive. Pi-essure between the fingers will excite
distinct positive electricity in piecesof transparent double-refracting
calc-spar. Topaz, aragonite, fluor'spar, ^arljouate of lead, quartz,
and other minerals show this property, but in a much smaller
degree. Some bodies remain excited much longer than others,
topaz for a very long time. Heat or change of temperature excites
electricity in many crystals ; as iu tourniahue, calamine, topaz, calc-
spar, beryl, barytes, fluor-spar, diamond, garnet, and others ; these
are hence said to be thermo- or pyro-eleatric Some acquire polar
pyro-eloctricity, or tlie two electricities appear in opposite parts of
the crystal, which are named its electric poles. Each pole is alter-
nately positive and negative, the one when the mineral is heating,
the other when it is cooling. Hankel's investigations of these
phenomena are specially noteworthy.
As already noticed, many polar electric minerals are also remark-
able for their hemimorphic crystal forms. Tourmaline, calamine,
and boracite are among the species thus affected. The polarity
continues so long as the temperature is increasing, and becomes
reversed when it commences to decline ; and wlien the heat is
stationary it disappears.
Rose and Reiss name one of the poles the analogue electric pole,
and the other the antilogne electric pole. Tlie former becomes
positive while the crystal is heating, and negative while cooling ;
the latter negative while heating, and positive while cooling.
^ecquerel found that in tourmaline at 30" C. electrical polarity
pas sensible; it continued undianged to 150^ as long as the
Ijgmperature continued to rise ; if the temperature remained
■fil 249. Fig. 250.
stationary an instant, the polarity disay.pearcd, but shortly mani-
foeted itself reversed, when the temperature commenced to decline.
If but one end of the crystal was heatwl tlio crystal was nnpohirized,
and when two sides were unequally heated each acquired an olcctii-
cal st.ite independent of the other. In tourmaline the extremities
of the prism arc dissiniilavly modified, and that end wliich pn
tlie greater number of planes is tlic antiloguo pole
if tht
niunner of puaes is the same, tne secondary rtiomboneorona ol tha
antiloguo polo have (one or more of them) loneer vertical axes than
those of the analomie pole. P"ig. 249 (tourmaline) ia tho antilogue
pole (negative unaer increasing heat), and fig. 250 tho analogue
pole. The pyramid of the analogue end ia more flattened by its
facets than that of the antilogue end ; thus e" and d^ of the anti-
logue end are more acumi-
nating than «' and tP of tht
analogue end- The same i;
the case with the other twc
crystals (figs. 251, 252).
Pyro-electricity has been \
observed in the following
substances : — tourmaline,
topaz, axinite, boracite,
Bcolezite, prehnite, electric
calamine, sphene, rbodizite,
heavy spar, rock-crystal.
Pyro-electricity ia of two
kinds,— either terminally
polar or centrally polar.
In the former the extre-
mities are opposite poles.
In the latter two sides of
a prism are of the same
name, and the opposite pole
to each is intermediate be-
tween the two.
The examples of the first kind are tourmaline, calamine, and
scolezito, which are uniaxal ; axinite, binaxal ; boracite and
rbodizite, with four axes. Calapiine, like tourmaline, has th«
sharper extremity the antilogue
end, and the more flattened the
analogue. Compound crystals
from Altenberg have both ends
analogue, and the portion which
lies between the twins antilogue
electric ; the pyro-electric axis
corresix)nds with the vertical axis
of the prism, as in tounnaline.
Boracite, which crystallizes in
cubic forms, with the opposite
solid angles differently modified,
has four pyro-electric axes, corre-
sponding to the four octahedral
axes. In fig. 253 of this species,
j^j, the pUne which has its angles modified by
V is the antilogue pole, and that with tho
Fig. 252.
Fig. 25a
Fig. 254.
unmodified angles the analogue pole ; and, generally, the antilogue
pole has either more numerous or larger facets. Rbodizite re-
sembles boracite in its pjTo-electricity.
The species in which pyro-electricity of the second kind has been
observed are ]>rohnito and toixiz. If fig. 254 represent a tabular
crystal of prehnite, tho poles will be situated as marked, the
analogue being central, and the antilogue at either extremity of
the shorter diagonal of tho rhombic prism. Topaz has in a similar
manner a central onaloguo polo, and an antilogue at either ex-
tremity of tho shorter diagonal. In some instances there is a
separate set of similar poles near one or the other angle, as in fig.
255 ; this must bo dne to tho crystals being ol a composite nature.
Magndisni. — This property is very characteristic of the Magiv*i
few minerals in which it occurs, — chiefly ores of iron or '*'"•
nickel. Some magnetic iron ores possess polar magnetism*
or are natural magnets ; while the conunon varieties of
magnetite, meteoric iron, magnetic pyrites, precious garnet,
and other minerals, are simply magnetic. Most minerals
are only attracted by the magnet, but do not themselves
attract iron.
Minerals, as other sub.stances, have also b«en divided into
magnetic and diamagnctic. See Magnetism.
Tho ordinary modo of testing whrtlicr a mineral is magnetic o*
not is to bring it near a pole of a delicately su.spended m.if'netio
MINERALOGY
377
stUe
jwlarty.
Hot
«QBd'J<
nvitj-
Sum-
aioDi's
Beadle, and dbeerre wbether it caiues it to vibrate. Another mode
if to apply a strong magnet to the mineral in powder. These are
gofficient for the minoralogist, Delesse has experimented exten-
rively npon the magnetic force of minerala, and has determined
the relative amount for numerous species. Calling this force for
Styrian steel 100, the following are some of his results : —
Natlm platlnnm _ _.. .—..--..... 2178 lo 3-047
liwnetic Iron ore -..- ___....™..16'00 to tSOO
rtvnUJDlte. from the United SUtea. .. «.. 1-0S8
CbromJc Iron - « . 0'186 to 0-0C5
Spinel (pleonaste), from HonzODt Tyrot - 0-078
Tlumic Iron {rhombohedral), often magnellpolar. 6764
Spocolar Iron, Bomettmea mai^ietipolar. ,..,_ 0'14 to 3*35
Graphite. 0015 to 0040
Spathic Iron (spheroslderlte, the hlgheat),...^.- 0*092 to 0-287
Iron pyrites » «.. 0-039 to 0-067
VlvUnlte. _. _...^._ -.. 0-027 to 0-076
Colomblte of Bodeamala and aaddam... 0-.161
Pyrochloro -.«.« 0-010
Chrysoprue (qnsrtz ]» dlamagnetlc, bat many Tarle- 1 (..ma
tlea •ro magnetic). _ f x <~«
Felapar, sometimes feeMy magnetic
Labradorlte of an antique green porphyry — 0-077
Hornblende OOU to 0067
Cri/stallomaffnetic Action. — The magnetic polarity thus
far alluded to belongs to the mass, and has no relation to
crystalline form. There is also a kind of polarity directly
related to the crystalline or optic axes of minerals. A
crystal of cyanite, suspended horizontally, points to the
north, by the magnetic power of the earth only, and is a
tme conipass needle, from which even the declination may
be obtained ; and the line of direction is the line of the
optic axes. Other crystals, which are called negative,
take a transverse or equatorial position. The latter are
diamagnetic crystals.
Conductivity for Seaz. — Senarmont found that the con-
ducting power of colloids and of crystals of the cubic
system is equal in all directions, but that it varies in
different directions in crystals belonging to all the other
systems, exhibiting characters analogous to those deduced
from their double refraction, conformable with the optic
aies of the crystal, and referable, as in the latter case, to
axes of elasticity, or unequal compression of the molecules.
The fundamental fact is easily shown by taking two slices of
loclc-crysfal, one cut transverse to the axis and one parallel to it
Through the centre of each plate a Bmall hole
is drilled for the reception of a bent wire,
which by insertion into the hole sustains the
{date. The other end of the wire is to be heated,
and the rate of the conduction of the heat is
rendered visible by the amount of a thin coating
of beeswax, with which the plate has been pre-
rioasly coated, which is melted round the central
hole. It will be seen that in the transverse slice
the wax is melted in a circular form, while in the
longitudinal slice the form is elliptical (fig. 256).
The conduction is equal in all directions, as
regards the transverse axes of the hexagonal
f>nsm, but more rapid in one direction in the
ongitudinal slice, and that direction is the line
of ita optic axis. In the case of quartz the two
diameters of the ellipse are as 1000 to 1312.
If the regular disposition of the molecules of
amorphouslmdies be interfered with by unequal
tension or compression, the regularity of their
power of conducting heat is destroyed, and they
also show elliptical forms of melted wax ; and
the ahorter axis of the ellipse is in the line of
pressure or undue packing of the molecules.
The heat thus does not travel so fast in this
direction, — partly because it is spent in the
heating up of the greater number of molecules. Hence -we might
conclude tnat along the main axis of quartz a smaller number of
molecules are packed in an equal space than along the transverse.
The following are the more important of Scnarniont's results.
1. Crystals of the tetragonal and rhombohedral systems have one
axis of conductivity which is either greater or smaller than the
others, and this axis coincides with the main crystallograpbic axis.
The isothermal surfaces are ellipses which lie in the line of this
axis, and these ellipses may be either elongated or flatteued in
the direction of this line.
2. In crystals of the right prismatic system the isothermal
surfaces have three nneoual .ixes, which coincide with crystallo-
gniphic ^es drawn parallel to the edges of the rectangular prism.
S. In crystala of the oblique rhombic system the isothermal
Fig. 256.
surfaces have three unequal axes, one of which coinddea with the
horizontal diagonal of the base, while th£ other two have directions
which art: not referable to any law.
4. In crystals of the anorthic system the isothermal surfaces
have three unequal axes, all with indeterminable positions.
In crystals of a single axis there appears to exist Do constant
relation between the axis of optic elasticity, whether maTimnm or
minimum, and the axis- of the greatest or of the least calorific
conductibility. Thus, of the minerals examined by Senarmont,
quartz ( + ), calcito ( - ), cassiterite ( + ), rutile ( + ), and calomel
( + ) have all their greatest axis of conductibility parallel to the
principal axis ; idocrase, beryl, tourmaline, and corundum, all
optically negative, have on uie contrary their smallest axis of
conductibility parallel to the axis.
In crystals belonging to the obliq^ae rhombic system there is
rarely coincidence between the thermic axes and the axes of optic
elasticity. In gypsum and in felspar these lie apart to a marke'*
extent
Dilatation by Heat. — In crystals of those systems in whicn Ditota-
the molecules are arranged unequally as regards their ares, *'<*•
the amount of their dilatation when heated is unequal in
the direction of their axes. Our knowledge of this subject
is chiefly due to MitscherUch.
In crystals of cubic sjrmmetry the expansion is equal in all
directions. The dimetric systems — the pyramidal and hexagonal —
are brought together as regards this quality, inasmuch as the axes
of volumetric change are in these the same ; for, while these in
the pyramidal correspond with the crystallographic axes, in the
hexagonal the three axes are the vertical, one lateral axis, and an
axis lying intermediate to the other two and at right angles to the
first lateral axis. The expansion along the principal axis may be
either greater or less than along the othere ; and in some minerals
there is even contraction along one axis.
In the right prismatic system the axes of dilatation correspond to
those of form. In the oblique prismatic one axis corresponds with
the orthodiagonal, but the others make angles not only with the
other crystaBographio axes but, strange to say, vrith the axes both
of thermic conductivity and of optic elasticity. We aro as yet
ignorant of the properties of anorthic crystals in this respect.
As a consequence of this unequal expansion along different axes,
the angles of crystals, other than those of the cubic system, are
altered under the influence of heat The alteration is extreme in
the case of calcite, where, through elongation along the vertical
axis, with some concomitant contraction of the transverse, the
angle of the rhombohedric faces is, when the crystal is heated
from 32° to 212° F., diminished from 105° 5' to 104° 66' 23",—
the form thus approaching that of a cube, as the temperature is
raised. .. . . v ,i ,tn
Dolomite, in the same range of temperature, diminishes * lo-
in some rhombohedrons, as of calc-spar, the vertical axis is lengthened
(and the lateral shortened), while in others, like quartz, the reverse
is true. The variation is such, either way, that the double refrac
tion is diminished with the increase of heat ; for calc.spar possesses
negative double refraction, and quartz positive. According to
Fresnel the same is true of gypeum. The dilatation for calc-spar,
according to experiment, is 0-001961.
Kopp has shown that in the carbonates of lime, magnesia, iron,
manganese, and zinc, which are nearly the same in the angle of their
crystals, the vertical axis is shorter the greater the atomic volume
And since heat diminishes the density, and therefore necessarily
increases the volume, the axis a should be lengthened by an increase
of temperature, as is actually the case. He has determined by cal-
culation that the change of angle from 32° to 212° -^— '-> '-' ' •"
■ should be 7' 37"
small as to he scarcely measurable, yet they may be sufficient fi
establishing a di*rence between substances which have identical
geometiic form while belonging to dilfeicnt systems of crystalliza^
tion. The angle of a rhomboliedron might at a certain temperature
he 90°, and so coincide with a cube ; but that angle would in Si
rhombohedron change whenever the temperature altered, while th»
angle of a true monometric cube is constant at all temperaturw:
The increase in volume and diminution in density which gencraUy
result from heating are always accompanied by a change in optical
properties. In trimetiic crystals, where the principal indices altar
nnequall)', the change affects the amount of divergence of the optio-
axes. The amount of alteration in gypsum, when the divergence
is diminished, is extreme. At the ordinary temperature the angW
of the divergence of the optic axes which be m the plane M
symmehy U about 90° for red light; when heated to 177 it la
diminished to 0°, and for the moment the crystal appears to Do
nniaxaL When more highly heated, the axes again diverge but
in a plane at right angles to the original one, and in cooling tnese
changes take place in reverse order. In barytea and celestine again,
the alteration in the angle of the optic axes is a divergence when,
heated.
16—15*
378
MINERALOGY
TeuMity,
Characters depending on Cohesion.
These characters are of five kinds : — (1) hardness, (2)
tenacity, (3) elasticity, (4) cleavage, (5) fracture. All may
be considered as related to the power of resisting attempts
to separate one part from another.
1. Hardness. — A harder body is distinguished from a
softer, either by attempting to scratch the one with the
other, or by trying each with a file. Each of these methods
is used by the mineralogist in determining the hardness
of the species, though the latter is in most cases to be
preferred. Both methods should be employed when
practicable.
Certain varieties of some minei'als give a low hardness under the
file, owing eitlier to impurities or imperfect aggregation of the
particles, while they scratch another mineral upon which a file would
have no effect, showing that the particles of the first are hard, though
loosely aggreo;ated, Chiastolite, spinel, and sapphire are common
examples of this. "When the mineral is too hard to be impressed by
a file, the peculiarity of the grating sound will suffice for the prac-
tised ear.
Mohs introduced a scale of hardness, consisting of ten minerals,
which gradually increase in hardness from 1 to 10. The intervals
between 2 and 3 and 5 and 6 are larger than the others. Breithaupt
has therefore introduced another degree of hardness between each
of the above, and thus his scale consists of twelve minerals.
The scale is as follows : —
1. Talc, common laminated light green variety.
2. Gypsum, a crystallized variety
2'6. Mica (muscovite).
5. Calcite, transparent variety.
4. Fluor-spar, crystalline variety.
6. Apatite, transparent variety.
C*6. Seapolite, crystalline variety,
6. Felspar (orthoclase), white cleavable variety.
V. Quartz, transparent.
6. Topaz, transparent.
9. Sapphire, cleavable varieties.
10. Diamond.
If the file abrades the mineral unaer trial with the same ease as
Ko. 4, and produces an equal depth of abrasion with the same force,
its hardness is said to be 4 ; if with more facility than 4 but less
than 5, t'ne hardness may be i\ or 4^, written in decimals 4"25, 4'5.
Several successive trials should be made to obtain certain results.
The use of the file is acquired with very little experience ; usually
a single trial is sufficient. Care must be taken to apply the file to
edges of equal obtuseness. That part also of the specimen should
be selected which has not been altered by exposure, and has the
highest degree of transparency and compactness of structure. The
pressure for determination should be rather heavy, and the file
should be passed three or four times over the specimen.
Where tlie scale of hardness is wanting, or a first rough deter-
mination is sought, the following experiments may serve ; —
Every mineral that is scratched by the finger-nail has H. =-2'5 or
leas. Minerals that scratch copper have H. — 3 or more. Polished
white iron has H. -4'5. Window-glass has H. =6 to 5-5. Steel
point or file has H. =6 to 7 ; hence every mineral that will cut or
scratch with a good penknife has H. less than 6. Flint has H. -7,
and only about a dozen minerals, including the precious stones or
gems, are harder.
Many specimens present different degrees of hardness on dis-
similar faces ; as an example of which we mention cyanite and
mica. This is confined to the inequilateral primary forms, and like
the similar difference of colour, lustre, &c., finds a ready explana-
tion in the theory of their formation; unlike faces are the result of
the action of a polar force acting along unlike axes.
This difference in faces parallel to unlike axes may be perceived
in nearly all cases, when the methods of trial are sufficiently
delicate. Huygens obser\'cd long ago that the cleavage face of a
crystal of calc-spar differed in hardness from the other faces ; and
even in a monometric crystal it has been found that the faces of
■the cube and octahedron are not exactly alike in this respect.
2. Tenacity. — Solid minerals are said to be brittle,
eectile, malleable, flexible, or elastic : —
1. Brittle, when parts of a mineral separate in powder or grains
on attempting to cut it ; as baryte, calc-apar.
2. Scdik, wlien pieces may be cut off with a knife without fall-
ing to jTOwder, but etiU the mineral pulverizes tinder a hammer;
as Drucite, gypsum.
8. Malleable, when slices may be cut off, and these alices
flatten out under a hammer ; as native gold, native copper.
4. Flexible, when the miueral will bend and remain bent after
the bending force is removed ; as gypsum, graphite, talc.
[ 6. Elastic, when after being bent it will spring back to id,
original position ; as mica.
A liquid is said to be' viscous when, on pouring it, the
drops lengthen and appear ropy ; as petroleum.
3. Elasticity. — Investigations on this property have n6t Etj-itidty,
to any extent been entered upon. The unequal elasticity
of unlike faces of crystals has been shown by Savart in his
acoustic investigations, and he was able to distinguish the
rhombohedral from the other faces in the pyramid of quartz
crystals ; he also showed that the figures formed upon
vibrating plates of crystals were directly connected
with their optic axes. Milne, by measuring the amount
of recoil of a sphere of calcite when struck at different
points by another of rock-crystal, found that the elasticity,
as thus measured, was greatest along the line of the optio
axis, and least in directions at right angles to it. . He also
found that points which lay intermediate between the main
and the transverse axes were most indented by the blows.
This goes to show that, although there may be fewest
molecules arranged along the lines of the transversa axes,
yet cohesion operates with greater intensity along these
than in intermediate directions.
When the tenacity of a mineral is overcome by an over-
whelming amount of traction, or its elasticity by a sudden
shock, its parts are separated, either in flat and continuous
surfaces, or in siu-faces which are irregtilar in the extreme.
The first of these modes is termed cleavage, the second
fractm-e. In those substances in which cleavage exists it
is found that the planes or directions along which it takes
place lie in certain strictly definite positions to one another
and to the axes of the crystal. They show not the smallest
tendency to a transition or gradual passage into the other
directions of greater coherence.
4. Cleavage. — The number of these parallel c'.eavaga- Cleir:'^
planes is altogether indefinite, so that the only limit that
can be assigned to the divisibility of some minerals, as
gj'psum and mica, arises from the coarseness of our instru-
ments. These minima of coherence, or cleavage-planes, are
always parallel to some face of the crystal ; and .-limilar
equal minima occur parallel to every other face of the same
form. Hence they are always equal in number to the faces
of the form, and the figures produced by cleavage agree
in every point with true crystals, except that Uiey are
artificial. They are thus most simply and conveniently
described by the same terms and signs as the faces of
crystals.
Some minerals cleave in several directions parallel to the faces of
different forms, but the cleavage is generally more easily obtained
and more perfect in one direction than in the others. This com-
plex cleavage is well seen in calc-spar and fluor-spar, and very
remarkably in zinc blende, where it takes place in no less than six
directions. As in ea(ih of these the division may bo indefinitely
continued, it is clear that no lamellar structure in any proper sense
can be assigned to the mineral. All that can be .itfirracd is that
contiguous atoms have less coherence along a direction normal to
these planes than in other directions. When cleavage takes place in
three directions, it of course produces a perfect crystal form, from
which the system of crystallization and angular dimensions of the
species may be determined ; it '« thus often of very great im-
portance.
The common cleavage in the different systems is as follows, those of
most frequent occurrence beingin italics :— (1) In the cubic system,
Octahedral, 0, along the faces of the octahedron ; HexahedraZ,
ocOoo , along those of the cube ; and Dodecahedr:.!, ccO. (2) In the
tetragonal system, Pyramidal, P, or 2Poo ; Prismalic, ooP, or ooPoo :
OT Basal, OP. (S) In the hex.agonal system with holohcdral form-s
Pyramidal, P, or P2 ; Prismatic, ooP, or ooPoo ; or Basal.OV; with
rhombohedral forms, Ithombclccdral, R ; Prismatic, ooR ; or Basal,
OR. (4) In the right piismatic system, pyramidal, P; Prismatic,
osP ; Maorodomatio .or Brachydcinatic, Poo or Poo ; Basal, OP ;
Macrodiagonal, a>Vx ; or Brachydiaqoruxl, ooPoo . (5) In tho
oblique prismatic system.Hemipyramidol.P, or- P ; Prismatic, coP;
Clinodomatic, P'eo ; Hemidomntic, P^co or-P°»'; Basal, OP;
Orthodiagonal, ooP»oo ; or Clincdiar.onal, coP'oo. <6) In th«
MIIi£RALOGY
379
•aorthic system, Hemiprismatic, ooP', or qoP ; Hemidomatic either
along the macrodome or the brachydome: Basal, OP ; MacrodiagoDal,
nf IS ; or BTOchydiagtmal, toPoo .
2 In some minerals, as mica and gypsum, the cleavage is
idily procured ; these may be held in the hand and
divided by a knife. Others only cleave with more or less
difficulty ; these must be placed on a firm support resting
on lead, folded paper, or cloth, and a sharp blow struck on
a chisel applied in a proper direction. This may often be
ascertained by examining the specimen in a strong light.
Sometimes it is necessary to subject them to extreme com-
pression in a vice. Some of the hardest substances have
not only a perfect but a facile cleavage, — as euclase, topaz,
and diamond ; many of the softest species have none. The
planes produced also vary much in their degree of perfection,
being highly perfect in some, as mica and calc-spar, and
imperfect in others, as garnet and quartz. In a very few
crystalline minerals cleavage-planes can hardly be said to
exist. Cleavage must be carefully distinguished from the
planes of union in twin crystals, and the division-planes of
laminar minerals,
re. 5. Fracture. — This is the irregular manner in which
substances may be broken. Even minerals possessed of
cleavage may be fractured in other directions ; but in
amorphous bodies fracture alone occurs. The following
varieties of fracture occur, and are highly characteristic: —
1. Conchoidal, almost typical of amorphous bodies, but occas-
sionally seen in crystals, — rounded cavities, more or less deep. The
name is taken from the resemblance to the successive lines of
interrupted j^owth in a bivalve shell. Seen in flint, obsidian,
asphalt. In calcite the direction of this fracture is intermediate to
the pianos of the mineral's cleavage.
2. Even, when the surface of fracture is smooth and free from
*nequalitics.
3. Jiovgh, when the surface of fracture is rugged, with numerous
small elevations and depressions.
4. SplinUry, when covered with small wedge-shaped spiinters.
5. Hackly, when the elevations are sharp, slightly bent, or
jagged, as broken iron.
6. Earthy, when it shows only fine dust
TasU, Odour, Touch.
Taste belongs only to soluble minerals. The different
kinds adopted for reference are as foOows : —
1. Astringatt, the taate of blue vitrioL
2. Sweetish astringerU, taste of alum.
5. Saline, taste of common salt.
4. AlkaliTU, taste of soda.
6. Cooling, taste of saltpetre.
6. Bitter, taste of epsora salts.
7. Sour, taste of sulphuric acid.
8. Pungent, taste of sal-ammoniac.
9. Metallic, taste of zinc sulphate.
Odour. — Excepting a few gaseous and soluble species,
minerals in the dry unchanged state do not give off odour.
' By friction, moistening with the breath, and the elimina-
tion of some volatile ingredient by heat or acids, odours are
sometimes obtained which are thus designated : —
1. Alliaceous, the odour of garlic. Friction of arsenical iron
elicits this odour ; it may also bo obtained from any of the arsenical
ores or salts by means of heat.
2. Eorse-radish odour, the odour of decaying horse-radish. This .
odour is strongly perceived when the ores of selenium are heated.
3. Sulphurous. Friction will elicit thia odour from pyrites, and
heat from many sulphurets.
4. Bituminous, the odour of bitumen.
5. Fetid, the odour of sulphuretted hydrogen or rotten eggs. It
is elicited by friction from some varieties of quartz and limestone.
6. Argillaceous, the odour of moistened clay. It is obtained
from serpentine and some allied minerals after moistening them
^with the breath ; others, as pyrargillite, afford it when heated.
7. Empyreumatic or ozonic. Quartz, when two portions strike
jpne another.
Touch. — Some minerals are oistinguished by a greasy
. Tfeeling, as talc ; others feel smooth, as celedonite ; others '
meagre, like clay ; others cold. This last character distin-
guishes true gems from their imitations in glass. Some, in
>rtue of their hygroscopic nature, adhere ti"> th« tongue.
Chemical Pkopeettes of Minerals.
Influence of Chemical Composition on the External Kelt' on •
Characters of Minerals. — That the characters of a com- comi-«i
pound must to a certaih extent depend on those of its*'""*^
component elements seems, as a general proposition, to prJ™'4i-s
admit of no doubt Hence it might be supposed possible '
from a knowledge of the composition of a mineral to draw
conclusions in reference to its form and its other properties ■
but practically this has not yet been effected
The distinction between the mineralizing and mineralizable or
the forming and formed elements lies at the foundation of all such
inquiries. Certain elements in a compound apparently exert more
than an equal share of influence in determining its physical pro-
perties. Thus the more important non-metallic elements, as oxygen, <
sulphur, chlorine, fluorine, are remarkable for the influence tiiey
exert on the character of the compound. The sulphurets, for
example, have more similarity among themselves than the various
compounds of one and the same metal with the non-metallic bodies.
Still more generally it would appear that the electro-negative
clement in the compound is the most influential, or exerts the
greatest degree of active forming power. After the non-metallic
elements the brittle, easily fusible metals rank next in power ; then
the ductile ignoble metals ; then the noble metals ; then the brittle,
■difficultly fusible ; and, last of all, the metals of the earths and
alkalies.
Generally each chemical substance crystallizes only in one form or
series of forms. Some substances, however, show dimorphism, or
crystallize in two forms, and thus may compose two or more minerals.
Thus sulphur, which in nature usually crystallizes in the right
prismatic system, when melted forms oblique prismatic crystals.
Carbon in one form is the diamond, in another graphite; carbonate
of lime appears as calc-spar and as aragonite ; the bisulphuret of iron
as pyrite and as marcasite. An example of trimorphism occurs in
titanic acid, forming the three distinct species anatase, rutile, and
brookite. It is remarkable that of dimorphic minerals one form is
almost always right prismatic; thus: —
Rhombic Form.
Cyanlte, anorthic.^ SUUmanltc, Andalualte.
Calc-spar, hexagonal Araffonlte.
Sasannlte, do ^ LeadhiUite.
AnSie }pr"">iiaal Brookite.
Pyrolnsite, right prismatic Folianite.
Cupiitc, cubic Chalcotrlchite (?)
SenarmoDtite, cubic ..„ VaJentinite.
Pyrite, do .,.,.».„.„.„ Marcasite,
Rammelsbergite. do Chioanthite.
Argcntite, do „ Acanihile.
Freiesiebenite, oblique prismatic Diaphorite.
Sulphur, do. Sulphur.
Even the temperature at which a substance crystallizes influences
its forms, and so far its composition, as seen in aragonite, Glauber
salt, natron, and borax.
Isomorphism. — Still more important is the Qocirine of laonnw
isomorphism, designating the fact that two or more simple or phisjn.
compound substances crystallize in one and the same form, or
often in forms which, though not identical, yet approximate
very closely. This similarity of form is generally combined
with a similarity in other physical and in chemical properties.
Among minerals that crystallize In the tesseral system,
isomorphism is of course common and perfect, there being
no diversity in the dimensions of the primary form ; but
for this very reason it is generally of less interest. It is of
more importance among crystals of the other systems, the
various series of which are separated from each other by
differences in the proportions of the primary form. In!
these perfect identity is seldom observed, but only very
great similarity.
The more important isomorphic substances are either simple sub-
stances, as (1) iluorine and chlorine; (2) sulphur and selenium; (3)
arsenic, antimony ; (4) cobalt, iron, nickel ; (5) copper, silver,
mercury, gold (?); or combinations with oxygen, as (6) lime,
magnesia, and the protoxides of iron, manganese, zinc; (7) sesqui-
oxides, as of iron, manganese, chromium, and alumina ; (8)
phosphoric acid, vanadic acid, arsenic acid; (9) sulphuric, selenio,
chromic acids; or combinations with sulphur, as (10) sulphuret of
iron and of zinc; (11) sulphuret of antimony and of arsenic; (12)stil-
phuret of lead, of copper, and of silver. These substances are named
vicarious from the singular property that in chemical compounds
they can mutually replace each other in definite proportions, and'
very often without producing any important change in the form or
other physical properties. But there are numerous instances among
the silicates where the mutual replacement of the isomorphio
380
MINERALOGY
1[»cldic9. esprri illy when the oxides of the heavy metals come in the
room of thr earths and alkolii's, cxt-rts a most essential influenre on
the external aspect of the species, particularly in regard to colour,
specific gravity, and transparency. The varieties of hornblende,
aiigito, carnet, epidote, and many other minerals are remarkable
proofs of this influence. This intermixture of isomorphic elements
confers many valuable properties on minerals, and to it this depart-
ment of naturp owes much of Its variety and beauty. Without the
occasional presence of the colouring substances, especially the oxides
of iron and manganese, the non-metallic combinations would have
exhibited a very monotonous aspect. It is also remarkable that in
some silicates the substitution of a certain portion of the metallic
oxides for the earthy bases seems to bo almost a regular occurrence;
whilst in others, as the felspars and zeolites, this rarely happens.
This fact is also of great economic interest, as drawing attention to
important elements often combined with others of less value. Thus
iron oxide and chrome oxide, sulphuret of copper and sulphuret of
(diver, nickel and cobalt, may bo looked for in connexion. The
fmeral chemical formulae for such compounds is formed by writing
( — radical or basis) for the whole isomorphic elements; and lu
special instances their signs are placed one below the other, con-
nected by a bracket, or, as is more convenient, are enclosed ii
brackets one after the other separated by a comma. Thus tho gene<
ral sign for the garnet is K3Si2+ fiSi, which, when fully expressed,
becomes {Ca^ Fcg, Mgg, Mug) Si2 + ('A'l, Fe, er)Si; and this mineral
forms many varieties as the one or other element preponderates.
Of the forms special to similar groups of atoms the more notable
are — the cubic system, special to metals proper, and binary
compounds as protoxides and haloid salts; the tetragonal to
binoxides ; the rliombohedral to carbonates; the hexagonal t»
sesquioxides and phosphates and their isomorph.s; the prismatic
to sulphates and tlieir isomorphs.
The isomorphism of minerals goes as a whole to show tliat form
depends on the number of molecules present, and is comparatively
little influenced by th,e nature of the molecules themselves
DESCKIPTION OF MINERAL SPECIES.
Bi-valcnt
elements.
The arrangement adopted in the following description
of mineral species is chemical. Simple substances are
considered first, in the order of their quantivalence, then
binary compounds, and la.stly those of more complex
structure. Our limits permit of the briefest notice of
the less important, in order that more space may be avail-
able for the delineation of the characteristic and transition
forms of such as go to constitute the more important rock
masses.
The following abbreviations are used: — H., hardness ;
G., specific gi'avity (distilled water at 60° Fahr. and
barometer 30 inches =1); cl., cleavage; sol., soluble;
8. \h. or n.] acid, sulphuric [hydrochloric or nitric] acid ;
' B.B., before blowpipe ; ox., oxidizing ; red., reducing ; c.c,
chemical composition ; com., combination.
In the chemical formulie, barred letters express two
equivalents, and the dots over the symbols indicate the
combination with them of as many equivalents of oxygen
as there are dots.
In the symbolic notation the several faces of crystals
are separated by semicolons, and the constituent members
of combinations by commas. The lettering on the faces of
the figures is for the most part that adopted by Miller.
In the enumeration of crystal forms, that which is typical
of the mineral is placed first.
SIMPLE SUBSTANCES.
1. SuLruuB, S.
(a) Right prismatic. P (p) polar sdges 106° 38', 84° 58', middle
edge 143° 17' ; ooP 101° 58'; OP (c) ; 5P(s); P«> (")• CrysUls
pyramidal, single or in druses ; also stalactitic, disseminated,
and pulverulent. Cl. basal and coP, H. = l'5to
2-5; G. -l-g to 2-1. Fracture conchoidal or
splintery ; biittle, sectilo. Lustre resinous, streak
aud colour sulnhur-yellow, passing into red, brown,
or gveeu, Suoliraes in the closed tube. Fuses a
little above the temperature of boiling water.
Takes fire at 513° F., and burns with a pale blue
flamo with odour of sulphurous acid. Co.: pure
sulphur, occasionally mixed with traces of selenium,
and when amorphous with clay or bitumen. Found Y\rr 257
chiefly in Tertmry strata. Localities: Girgenti in °'
Sicily, with celestine ; Conil in Spain ; Bex in Switzerland ; Cracow
in Poland ; deposited from hot springs in Solfatara near Naples ;
from hot springs in Iceland ; from sulphur springs in New York ;
and in cavities of decomposing galena, cinnabar, and pyrites at
several localities.
(6) Oblique prismatic. The crystals of volcanic sulphur are of
this form ; they occur in the neighbourhood both of extinct and of
recent volcanoes. They are slender, needle-shaped, and interlacing,
and have generally more or lt:ss of a red-brown tinge. Oxhavecr
and Capo Rcykjanes in Iceland, Sicily, and the volcanoes of
the Pacific, the Chilian Andes, and California yield this variety.
2. Sklensulphur, S.So.
Like sulphur, but rcddisli brown to orange-yellow. B. B. burns
with fumes of s^leniuus acid mixed with the suljdiurons. Found
ill tho crater of Volcano iu the Linari Islands, and Kilauca in
Hav.-i'
^S
3. Selenium, Se.
H. =2; G. =4'3. Broivnish black to lead-grey; thin splinters
translucent and red. From Culebras in Mexico.
4>. Tellurium, Te.
Rhombohedral ; R 86* 50'. In minute hexagonal prisms, with
basal edges replaced ; usually massive and granular. Cl. lateral
perfect, basal imperfect. H.=2to 2'5; G.^-S'l to 6'3. Tin-white;
sectile. C.c: tellurium with a little gold and iron. Occurs at
Facsebaya near Zalatbna (Transylvania)^ and in several mines iu
Boulder county, Colorado ; masses 25 lb in weight have been obtained
there.
5. AnsENic, As.
Rhombohedral ; R 85" 36' (fig. 258). Usually in botryoidp.l Trl-TiOort
investing masses composed of numberless layers. The structure is ekiiratfc.
fine granular, rarely columnar. H. ■= 3 '5 ; G. = 5 7 to 5 '93. Cl. basal
Colour black and dull, but when fresh broken very
splendent and silver-white ; fracture uneven.
AVhen rubbed or heated gives out a l.
odour. B. B. volatile, with formation of white fumes.
C.c; arsenic, with some antimony, and traces of _.. ^^
iron, silver, and gold. Andreasberg in the Marz, *®'
Annaberg, Schneeberg, Freiberg, Joachimsthal, Allemont (Dan
phin^), Kongsberg (Norway), the Altai, Chili, Pebble mine (Dum,
friesshire), Tyndrum (Perthshire).
6. Antimony, Sb.
Rhombohedral ; R 87* 35' ; but rarely crystallized, generally iu
foliated or granular masses. Cl. basal. H. =3 ; G. =6-6 to 6-8. tin-
white, with slight yellow tarnish. Brittle and sectile. B.B. easily
fusible; volatilizes, and on charcoal leaves a white deposit, burning
with a p£-le flame. Found at Andreasberg, Przibram (Bohemia),
Sala (Sweden), Allemont, Southham in East Canada, and Borneo.
7. Allemontite, SbAsg.
Hexagonal, spherical, reniform, and investing. H. ™3*5 ; G. = 6"!
to 6 "2. Lustre, when fresh, metallic. Tin-white to lead-grey, but
with a blue or brown tarnish. B.B. strong odour of garlic, with
residuum of oxide of antimony. C.c: antimony 87 "85, 'arsenic
62'15. Almost always in curved foliated Inminoe. Occurs at
Allemont, Przibram, bchlaJmine in Styria, Audreasbefg.
8. Bismuth, Bi.
Rhombohedral ; R 87° 40'. Crystals, R,OR, generally distorted ;
also reticulated, spear-head twins, or arborescent ; also disseminated
andgranular. Cl. basal, perfect. H. -2-5 ; G. -9-6 to 9-8. Brittle
aud sectile. Reddish white, often tarnished grey, brown, or blue.
B.B. easily fusible, even in candle flame. Volatilizes on charcoal,
leaving a citron-yellow crust. Sol. in n. acid ; solution pre-
cipitated when tlirown into water. Occuj-s in gneiss and clay
slate in veins and disseminated, along with ores of cobalt, silver,
load, and zinc. Alva in Stirlingshire, Cumberland, Devonshire
and Cornwall, Schneeberg, Slarienberg, Joachimsthal, Biobcr,
Modum (Norway), Falun (Sweden), Bolivia.
9. Telluric Bismuth, BiaTcj.
Bismuth 52, tellurium 48. Virginia, Dahloncga in Georgia, Mon-
tana. A variety witli 7 per cent, of selenium am* H. -2 also
occurs.
10. Tethadymite, BijTojS.
Rhombohedral ; 3R 68" 10'. 'Almost always twins of SR aud
OR, with tho faces of OR at 93". Cl. basal, perfect. Sectile, and thin
laminiE flexible. H.-l to 5 ; O. -72 to 7-6. Steel-grey. B.B.
fuses, yielding a grain of metal which ultimately volntilizes. SoL
iu n. acid. C.c: 596 bisnuitii, GTrO tellurium, aud 4 3 sulphur.
I Schemnitz.
MINERALOGY
381
11. WxHBUTi, Bi(Te,S).
HexacoiuL CL basal. H.-l to2; G. 'S'4'i. Highlastre. Steel-
jroy. C.C.: bismnth 61 "15, teUariuni 2974, sulphnr 233, silver
S'07. Deutsch-Pilseu in Hungary.
12. JosEITE, Bi,Te,(SSe), .
Hexagonal. CL" basaL Q. — T'SS. Colour grey-black to steel-
grey. Brittle. C.c: tellurium lB-93, sulphnr 316, selenium 1-48,
bismntli 79 15. San Josi (Brazil). A Cumberland variety
yielded tellnrium 673, sulohnr 6-43, bismuth 84 '33, corresponding
to Bi/TeS,).
18. DlAUONS, C.
Tar. 1. Crystallixed. — Cubic ; very frequently hemihedral.
Crystals most generally with curved facea. Twins common on the
octahedral face ; hemitropes also common (see figs. 170, 204, 205,
207). Crystals vary remarkably in appearance (see figs. 259 to 262).
CL octahedral. H. -10iG.-8-6to3-6. Transparent, or translucent
when of dark colour. Befracts light strongly. The back planes of
diamonds reflect all the light which strikes them at an angle exceed-
ing 24* 13', and thence comes their peculiar brilliancy. High
adamantine lustre. Colourless, but often tinged white, grey, and
brown, — more rarely yellow, pink, blue, green, and black, those last
named being the rarest Disperses light highly, and hence emits
brilliant flashes of all the colours of the spectrum. Becomes posi-
tively electric by friction. B. B. infusible, hut biims into carbonic
Fig. 259. Fig. 260.
icid in oxygen gas. When air is eicloded is unchanged at the
temperature of melting cast iron, but at that of melting malleable
iron is changed into a black coke, or, it is said, into graphite.
Insoluble in all acids and alkalies. C.c: carbon, with traces of
fiilica and earths. Geologic formation apparently a laminated
flexible quartz rock called itacolumite, whica occurs in Brazil, the
Urals, Georgia, and North Carolina, in the vicinity of places where
diamonds have been found. Minute crystals have been found in
zanthophyllite, and in talc slate and serpentine, in the Schischim-
skian hills, near Zlatoust (Russia). They have also been obtained
in Brazil imbedded in a conglomerate composed of much-worn
pebbles of quartz, chalcedony, and gold, cemented by limonite or
Fig. 261. Fig. 262.
ferruginous clay. In South Africa tiey are imbedded ia a steatitic
clay. Biamonda were formerly obtained in India, at Panua, Raol-
eonda, and Golconda. So few are now obtained here that the mines
are let for £1 a year. From these mines were obtained not only
the Kohinoor, which was possibly the same as the great diamond
mentioned by Tavernier as having been seen Uy him in the pos-
session of the Great Mogul, which weighed 280 carats, but the
Regent, of 136 carats (which, not only from its size, hot from the
perfection of its form, is very much the finest diamond known), the
Nizam, an uncut diamond of 340 carats, and the Carlow, rose-
cut, 193 carats. More lately diamonds were found in great quantity
in the neighbourhood of Rio Janeiro in Brazil ; they occur in two
different deposits : the one called "gurgulho" consists of broken
quartz covered by a bed of sand ; the other, *'cascalho," consists
of rolled quartz pebbles united by ferruginous clay ; both rest on
talcose clays, which are the debris from talcose rocks. The first
deposit affords the finest diamonds, and both contain gold, plati-
num, magnetite, and rutile. A dodecahedral diamond ol 257
carat3 was lately found at Bogagem in this district; this wv
reduced by cuttmg to an oblong brilliant of 125 carats, and ii
the second most valuable dian-ond,— the Kohinoor, now reduced
to an imperfectly ciicuUr brilliant of 102 carats, occi^pvim; the
third place. Tho two c.iloared diamondii most worl'-v ,jf noU
are a green diamcind in the DTM>!cn collection weighing » carats,
which 13 a little deeper in imt than a beryl, and a blue diamond
in the Hope collection, of 44 carats, as highly coloured la a
sapphire, which it is by some considered to be. Diamonds have
lately been found in very large quantities, and some of great size
north of the Capo of Good Hope; these for the most part are of
yellow colour and of very inferior value. Wliile a Brazilian cut
brilliant of one carat is worth from £20 to £25, the value of
the finest brilliants from tho Cape is only from £3 to £4, and that
of the yellow diamonds is from £2 to £2, lOs. Apart from its
employment as an ornamental stone, the diamond has an intrinsic
value from its being utilized for cutting glass and for grinding i^i
polishing other gems. Of late years its usefulness has had a new
application, it being employed for the drilling of rocks in tunnelling
operations and in the boring of artesian wells. A singular observa-
tion has resulted from these last methods of utilizing it, namely,
that the hardness of the African diamonds, as tested by the amount
of their endurance, is markedly inferior to that of the Brazilian and
Indian. So much is this recognized that, while the bort, or
minute crystals, of the latter command a price of 15s. per carat, the
■African can be got for about 5s. The cleavage of certain of the
African diamonds is so eminent that even the heat of the hand causes
some of them to fall in pieces. Such diamonds, generally octahedra,
may be recognized by a peculiar watery lustre ; they are called plate
diamonds. The above facts give some ground for the supposition
that there may be a alight difference in their composition, possibly
that both may contain small, but different, quantities of hydrogen.
The circumstances under which diamonds have been formed are
altogether unknown. The fact of their being changed into a kind
of coke at a very high temperature is an argument against their
having been produced through the operation of heat, and it has long
been known that an excess of carbon dissolved by molten cast iron
crystallizes on cooling in the form of graphite ; yet the only attempts
to form diamonds deserving of bemg mentioned as having been
attended with any measure of success are those in which sugar
charcoal was dissolved in molten silver at the temperature only of
melting steel. There were thus obtained a few minute black and
also colourless octahed/al and cubo-octahedral crystals with curved
faces, mingled with a mach larger amount of graphitoidal carbon.
Var. 2. Massive. — In black pebbles or masses called carbonado,
sometimes 1000 carats in weight. H. -10; G. -3012 to 8-42.
C.c: carbon except 27 to 2 07 per cent of ash. Found in the
mines of Baranco, &c, in Bahia.
Var. 3. AnOnvcUic — Like anthracite, but scratches the diamond
In mammillar masses, partly in concentric layers, and globular.
Brittle. G. — 1'66. C.c: carbon 97, hydrogen -6, oxygen IS,
When cat and polished, refracts and disperses light, like the diamond.
Supposed from Brazil
.14. Graphitb, C.
Hexagonal in flat crystals ; p:p 85* 29'. tJsually foliated,
scaly, or compact CL basaL H. — 0"6 tol ; G. — 19 to 2'2. Lnstre
metallic. Colour and streak black to dark steel-grey ; flexible in
thin laminie; very eectile; feels
greasy ; leaves a mark on paper
of its own colour; conducts elec-
tricity. B.B. bums with diffi-
culty ; heated with nitre, de-
flagrates. C.c. : carbon, with
small quantities of volatile
matter, and ash from 6 to 40 per
cent Stratlifarrer (Invemess-sh
Borrowdale in Cumberland, Ural Mountains, Ceylon, Greenlan(L'
Used for making pencils.
15. Tin, Sn .
Tetragonal in greyish white metallic grains. Reported as occur-
ring with Siberian gold; with bismuthite from Guanajuato in
Mexico.
16. Iron, Fe.
Cubic; in grains and plates or disseminated. H. — 4"6; G. — Native
7 to 7 8. Steel -grey or iron-black. Fracture hackly, very metala.
magnetic B.B. infusible. SoL in h. acid. Two varieties
are to be distinguished, (a) Telhtric Iron, in grains and plates.
Almost pure iron, or contains graphite, carbon, lead, or copper, but
no nickel. At Chotzen in Bohemia in limestone ; in an argillaceous
sandstone in the keuper at Miihlhauscn ; in Thuringia along with
fossils ; in an ironstone con;;lomerate in Brazil, and in lava in
Auvergne ; in the mine of Hackenburg ; at Bexley, in Liberia,
Africa, along with quartz, a zeolite, and magnetite ; enclosed in
magnetite in Unst (Shetland) and in Sutherlandsliire ; in basalt ia
Antrim, Ireland; in the gold sands of Brazil, tho Urals, and Olah-
oisn (Transylvania). (J) ifetmric iron, steel-grey to silver-white.
Fig. 263.
shire). Mull, Cralgman (AyrshiteV
382
MINERALOGY
Almost always ctmtaina nickel, with cobalt, copper, and several
minerals which are non-terrestriiil. When polished and etched
with nitric acid the surface is marked by lines of unaffected inter-
lacing crystals called Widmannstatten's figures ; most of the nickel
is contained in these. Occurs in masses which vary in size from
the smallest microscopic dust as dredged from the depths of the
ocean to upwards of 32,000 lb. Mauy of these masses have been
seen to fall. Several (suspected, however, to be terrestrial) have
been found imbedded in a basaltic rock near Disco Bay in Green-
land, one of which is 44,000 lb in weight. Several contain
hydrogen in their pores, condensed to the extent of eight times the
volume of the mass; and the pitted depressions frequently observable
upon their surface give couutenance to the view that, if not dis-
charged frbm a volcanic throat, they were set at liberty by some
sudden disrupting gaseous explosion.
17. Zixo, Zn.
Khombohedral. Said to be found in large hexagonal pyramids.
Cl. basal, perfect. H. --2; G. -7. Lustre metallic. Colour and
streak bluish white. Found in a geodo in basalt near Melbourne,
Australia, coated with smithsonite, erythrine, and aragonite. Also
in the gold sands of the Mittamitta river.
18. Copper, Cu.
Cubic (figs. 28, 30, 26, 33, 37, 264). Twins, on an octahedral face.
Crystals genernlly distorted Often filiform and arborescent, or in
plates and lamins. H. =2'6 to 3; G. =8-5 to 8'9. Lustre dull
metallic. Colour and streak copper-red,
with yellow or brown tarnish. B.B. easily
fusible, colouring the outer flame green.
Sol. iA n. acid. Occurs in many rock
(generally igneous), and frequently asso-
ciated mth zeolites. In the Faroes, Uiist
(Shetland), Cornwall, Chessy near Lyons,
tlie Banat (Hungary), Siberia, China,
Mexico, Brazil, Chili, and Australia.
Masses of great size are found, much the
1 irgest being from the Ontauagon river,
on the south of Lake Superior. One Fig. 264.
mass found in February 1857 was 45 feet
in lennlh, 22 feet in width, and 8 feet in thickness; its weight was
420 tons. Another was found in 1869, 65 feet in length, 32 in
width, and from 4 to 7 feet in thickness; this weighed upwards of
1000 tons^ and had a value of 400,000 dollars.
19. Lead, Pb.
Cubic, but only in thin plates, capillary or filiform. Cl. none.
H.-1-5; G.=ir36 to ir4. Irtictile, malleable, and sectUe.
Bluish grey, but with a blackish tarnish. Found in lava in Madeira,
nnd at the mines near Cartagena in Spain ; in amygdaloid near
Weissig ; in basaltic tufa at Rautenberg in Moravia ; with gold near
Mount Alatau in the Altai, at Velika in Slavonia, and at Olahpian
in Transylvania ; near Ekaterinburg in the Urals; lu the distnct
of Zomolahuacan in Vera Cruz, in foliated galena, in granular lime-
stone ; in the iron and manganese bed of Paisberg in Wermland
(Sweden), with hseraatitc, magnetite, and hausmannite ; in white
quartz, north-west, near the Dog Lake of the Kaministiquia, an
affluent of Lake Superior ; imbedded in hornstone in plates and
grains, in the mine of Bogoslovskoi in the Kirghiz steppes; in gi-een-
stone porphyry at Stutzerbach in Thuringia ; with bffimatite in the
islands of Nias on the west coast of Sumatra.
20. Mercury, Hg.
Cubic. Occurs in small liquid globules in its gangue, but may
be sol idified at - 39°, when it forms octahedral crystals. G. - 1 3 -696
when liquid, 15'612 when solid. Lustre brilliant metallic; tin-
white. B.B. volatile, sometimes leaving a little silver. Readily
n. acid. Occurs generally in clay shales or schists of dif-
:es. The globules of mercury are usually found in rents
bar, or accompanjing calomel, at most of the localities for
nerals. Found at Idria in Carniolaand Almadcn in Spain,
it is obtained by washing a soft clay slate. In Transylvania
-.nd Galicia springs issuing from the Carpathian sandstone bear
along globules of mercury. At the Pioneer mine in California some
of the quartz geodes contain several pounds of mercury. At Cividale
in Lombardy it is found in an Eocene marl. It has also been
observed occasionally in drift, and has even been stated to have
been found in a peat bog.
21. Silver, Ag.
Cubic (figs. 26, 30, 83, 40, 37). Crystals generally small, also and
most fre<iuently filiform, arborescent, and in plates or crusts. These
either project into cavities, coat their surfaces, or ramify in a reticu-
lated manner throughout the mass of the rock. Twins of octahedral
and trapozohedral composition. Noel. If. —2-5 to 8; G. -lO-l
toll-1. Lustre metallic. Colonrandstreaksilver-wbitc, but generally
tarnished yellow, brown, or black. Malleable, ductile, andsectilo,
but less 80 than gold. B.B. easily fusible. Sol. in n. acid;
the flolution colours the skin block. C.c ; silver, with varying
sol.
ferent i
these
At Id
proportions of gold, platinum, mercury, copper, antimony, and
bismuth. The auriferous from Norway contains silver 72, gold 28 ;
from quartz reefs in Sutherland, silver 7r4, gold 28'tf. The
cupriferous from Courcy near Caen contains 10 per cent, of copper.
The antimoniaj from Bohemia contains 1 per cent, of antimony.
The mercurial from Kongsberg in Norway baa '4 of mercury, found
chiefly in veins in gneiss, clay slate, and limestone. Localities :
Alva and elsewhere in Scotland, Ballycorua in Ireland, and Cornwall
in England ; at Freiberg, Andreasberg, and Kongsberg ; along
with narive copper at Lake Superior ; in Mexico, in Peru, and in
the United States. The finest crystallized silver occurs at Lake
Superior, and at Kongsberg. At the last locality the crystals
are an inch in diameter, and are disposed on large filiform
brushes. Silver occurs in large masses; three of 436, 560, 812 lb
have been recorded from Kongsberg. A block which smelted
44,000 lb was for some years used as a table by Duke Albert on
his annual visits of inspection to the Schneeberg mine in Saxony.
A Mexican specimen was found of 400 lb; the mines of Huantaya
in Peru have yielded masses of 444 and 960 lb. Britain produces
annually about 760,000 cz. of silver, chiefly, however, from lead
ores. The value of annual produce for the whole world from all
sources is from 8 to 10 millions of pounds sterling.
22. ScHNEiDERiTE {Gold Amalgam), AujHgg.
Tetragonal four-sided prisms, easily crumbling, yellowish white
to white ; sometimes in grains the size of a pea. C.c. : gold 41 '63,
mercUry 68'37. Found at Mariposa in California. A variety
(An, Ag)3 Hgfl is found along with platinum in Columbia ; thifl
contains gold 38 '39, silver 5, mercury 57 '40.
23. Arqiterite, AggHg.
Cubic. In octahedra, also In grains and dendrites. G. — 10*8.
Like native silver, but softer. C.c. : silver 86 "5, mercury 13'5. From
Arqueros in Coquimbo, Chili. Kongshei-gite, AgigHg, occurs at
Kongsberg, with 95*1 of silver and 4*9 of mercury.
24. Amalgam, Ag. Hgg, andAgFgj.
Cubic (fig. 33, in combination with 40, SO, 41, 38). Cl. dodeca-
hedral. H.-3to3-5; a=10-6tol4. Colour and streak silver-
white. Fracture conchoidal, brittle, grates when cut. In closed
tube yields mercury and leaves silver. Sol. in n. acid. The first
variety (silver 34'8, mercury 65'2) occurs at Moschellandsberg
in the Palatinate, where the veins of mercury and silver intersect
one another; the second (silver 26 "25, mercury 7375) there,
and also at Allemont in Dauphine, Almaden in Spain, in
Hungary, and in Sweden. From Rosilla in Atacama (Chili)
Domeyko reports the following other compounds; AggHg^, silver
46*8, mercury 53"2, white and silvery ; AgHg, silver 55 1, mercury
44'9, granular and dull; Ag^Hga, silver 642, mercury 35 8; of the
last there is a mass weighing 22 tt) in the rausemn of Santiago.
25. Gold, Au .
Cubic (figs. 30, 26, 33, 40, 36) and more complex forms. Crystals
generally small and indistinct through elongation, assuming capillary
and arborescent shapes. Also in thin plates. Twins rare; twin face
octahedral. Frequently in rounded and apparently colloidal masses
impacted in clay, or loose in small grains (pipettes) rolling in the
bed of streams. Fig. 265 is of such a mass found in Sutherland.
No ch H. -2-5 to 3 ; G. -17 to 19*4. Lustre metallic, but fre-
quently dull and partly
coated with a brown crust.
Colour and streak yellow-
ish white to bright gold-
yellow. Malleable, ductile,
and sectile ; the purer
varieties the more so and
the softer.. B.B. easily
fusible. Sol. in aqua regia,
generally with precipitation
of chloride of silver. Solu-
tion yellow, stains skin
purple-red, with corrosion.
C.c. : gold, with silver from 72 to 20 per cent ; somotimes iron and
copper under 1 per cent. Found in beds and veins generally of
quartz in metamorphic rocks of a schistose nature, rarely in diorite
and porphyry, and very rarely in granite. Its general associate
is limonite, formed from decomposition of pyrite ; sometimes also
hfcmatite ond ningnetitc. Occui-s also in microscopic grains in
quartz, from which it is extracted by crushing and amalgamation.
The geologic range is from the Azoic to the Tertiary and Cretaceous,
as in CuUfornift ; but even in these more recent rocks the original
source must have been at least Palaeozoic. Of localities which yield
goli the following may be noticed : — the Leadhills in Scotland,
Wicklow in Ireland, Dolgelly in North Wales, Cornwall in
England ; Transylvania, Hungary, and Piedmont; the Urals,
Ekaterinburg, and India ; Kordofan, the coast opposite Madagas-
car, and the Gold Coast (the fame of which has been recently re-
vived) ; Minas Geraes in Brazil, Bolivia, North Carolina, and
MINERALOGY
383
Cslifornia ;. and more recently Kew Sonth Wales and Qaeenaknd
in Australia, Tasmania, and New Zealand.
Some of the largest single masses ofgoldfonnd in recent'times are
the following: — one of 22 oz, in Transylvania, of 28 lb in North
Carolina, of 20 lb in California, one of 96 lb troy near Miask in the
TJrals, and one of 181 lb 8 oz., which. yielded £8376, lOs. 6d., at
Ballarat, Australia.
The annual produce of gold from Australia is about 5 millions of
pounds sterling, of the United States about IS millions, and the
whole earth about 23 millions. •
The following snb-species may be noticed : —
1. SUctrvm. This name for the alloys of gold and sUver
wa« applied by Pliny, whenever the proportion of the latter
metal was one-l^th. An alloy of 2 gold and 1 silver contains 21 per
cent, of silver ; this is found in Sutherland. One of I to 1 contains
86 per cent, of silver, this last being the most usual proportion.
It occurs in Transylvania, in the Altai, and in Colombia. Its
colour is brass-yellow to yellowish white. G.— 12"5 to 15'5.
2. Porpezite, or Palladium Oold (mro-poudri), from Porpez in
Brazil, contains 985 per cent, of palladium and 4"17 of silver.
S. Hlwdium Geld, from Mexico(G. —15'6 to 16'8), contains from
84 to 43 per cent of. rhodium.
26. Platiitvm, Pt.
Cubic ; rarely in small cubes or octahedrons, usually in minute
scaly grains, sometimes cohering, and also in rounded lumps. No cL
H. — i to 4'6; G. — 17to 19. Lustre metallic. Colour and streak pale
■teel-grey. Malleable and ductile with difficulty, haying a hackly
fracture. When containing much iron, magnetipolar. B.B. in-
fusible. SoL iu aqua regia, but only when heated ; solution red ;
corrodes the skin. C.c: platinum, but never to a greater extent
than 86 "5 per cent. The remainder consists of iron, iridium, rhodium,
palladium, osmium, gold, copper, and a mechanical mixture of irid-
osmine. The iron exists in quantities varying from 4 '3 per cent, to
double that amount. Occurs in Brat^l in syenite ; near Popayan
(Colombia) in alluvium, associated with chromite, iridium, palla-
dium, gold, and copper ; in the Urals in alluvium derived from
crystalline rocks; and at Nijui-Tagilsk in serpentine along with
chromite. It is also found in Borneo, California, and Carolina, and
is said to have been found in the county of Wicklow in Ireland.
The sands of many rivers yield it in small amount. Platinum does
not occur in large masses. A masa in the Madrid Museum from
Condoto weighs 2^\ oz. ; masses have been found in the Urals from
11 to 21 lb.
Iron Plalina is a sub-species. This, which ha.s a composition
FoPt^, and contains from 11 to 13 per cent, of iron, is found at
Nijui-Tagilsk. G. — 14'6 to 16'8 ; H. — 6. It is magnetipolar, and
attracts iron much more strongly than an ordinary magnet.
27. PLATINIBIDnrM.
In minute silver- white grains. H. -6 to 7 ; 0. —16 '94 to 228.
Contains 55'44 platinum, 27 '79 iridium, 686 rhodium, 414 iron,
S'3 copper, '49 palladium. Is found in Brazil
28. iBIDtlTH, Ir.
Cubic (fig. 27). H. -6 to 7; G. -21 '57 to 23'46. CI cubic, traces.
Very slightly malleable. Silver- white to steel-grey. B.B. nn-
changcd. Insoluble in all acids. C.c. : 76 '8 iridium, 19 '64
platinum, 0'89 palladium, 1'78 copper. Found at Nijni-Tagilsk,
generally in minute grains. Is the heaviest known substance.
.4v(ii<<, sub-speciej. From Ava in India. C.c: 60 iridium,
20 platinum (according to Prinsep).
29. Palladium, Pd.
Cubic ; in minute octahedrons, and in grains. H. — 4 '5 to 5 ; G. —
ll'Stoll'S. Malleable. Light steel-grey. B.B. infusible. Slowly
dissolves in n. acid, forming a brown-red solution. C.c: palla-
dium, with a little platinum and iridium. From the gold sands
of Brazil, often in small plumose crystalline lumps. Also from St
Domingo, and the Urals. Does r '>t tarnish with sulphurous fumes.
30. Allopalladium, Pd,.
Hexagonal ; in small flat hexagons, d. basal, perfect Lustre
piright silvery. Colour pale steel-grey. From Tilkerode in the
Harz, with gold.
31. Nkwjanskite (,Osmxndium), IrOs (iridium 4978, osmium
BO'22) and IrjOs.
Hexagonal; P 124°. OP, P, ooP. Generally in flat scales.
CI. basal perfect H. -7; G.- 18 '8 to 19 '47. Lustre -metallic.
Colour tin-white. B. B. unchanged. Insoluble
in all acids. The analyses of this mineral give
quantities of iridium varying from 44 to 77 per
cent , and of osmium from 21 to 49. Ruthenium,
rhodium, and platinum make np the 100 parts.
The largest quantity of ruthenium is 8 '49, and
one variety from New Granada was found to contain no ruthenium,
tint 12'3 of rhodium, which is more than double its usual amount
OwQis Tvith platinum in Chooo (Colombia) ; at Newjansk and
several localities in the Urals, in Anstralia, in northern (Mifomis
(somewhat abundantly in gold sands), also in Oinada.
82. SISSERSKITE (Iridosmium), IrOs^ (iridium 19'9, osmium 80^)
and IrOsj (iridium 24'8, osmium 75 '2).
Rhombohcdral; R = 84''28'. H. -7'5 i G. = 21'12. Colourleail-
grey to bluish. B.B. becomes black, with strong odour of osmic
acid ; in flame of spirit-lamp shines strongly, and colours flame
yellowish red. Occurs in smUl quantity with newjanskite at all
its localities, and in proportionally larger quantity at Sissersk in the
Urals. It is used for pointing gold pens, and in the United States
sells at 60 dollars an ounce.
COMPOO'jftDS OF FLUORINE, CHLORINE, BROMINE,
AND IODINE (HALOID SALTS).
33. Fldobite {Fluor-spar), CaF .
Cubic (figs. 267 to 270, also figs. 31, 33, 36, 65, 66, 57, 68); also
divergent crystalline, granular, and compact. Cl. octahedral ;
fracture conchoidal ; trittle. H. = 4 ; G. ■?■ 3 1 to 3 '2. Transparent
to pellucid. Lustre vitreous. Colourless, but generally colomed
purple, blue, green, yellow, white, black, and pink. Sometime*
two or three colours disposed in layers in one crystaL Frequently
Fig. 256.
Fig. 269. Fig. 270.
phosphoresces with difl'erent tints of light, when heated. B. B . de-
crepitates and fuses to an opaque bead. Sol. in s. acid with evolution
of hydrofluoric add. C.c : 51 '3 calcium, 48'7 fluorine. Common
in veins, generally associated with metallic ores. Shetland, Suther-
land, on the Avon, and Ballater in Scotland; Cumberland,
Northumberland, Derbyshire, and Cornwall; Saxony, Bohemia,
Freiberg. Used to be turned into vases and other ornaments ("blue
John ") ; formerly employed as a flux, now for etching and obscuring
glass.
34. Yttrocerite.
In crystalline crusts. H. = 4to 6 ; G. -8'4 to3'5. Translucent;
vitreous. Violet-blue to grey or white. B.B. infusible. Evolves
fluorine when heated with sulphuric acid. C.c: fluorides of cerium,
yttrium, and calcium. Finbo and Broddbo near Falun (Sweden),
Massachusetts and New York.
35. Fluoceeite, CeF-HCcjF,.
HeiagonaL H. -4 to 5; G. -4'7. Opaque or translucent on the
edges. Pale brick-red or yellowish ; streak yellowish white. B.B.
infusible. In closed tube gives out hydrofluoric acid. C.c: 82 '64
peroxide of cerium, 1'12 vttria, 16'24 hydrofluoric acid. Finbo
and Broddbo.
36. Flupceeine, CejF,-f(Ce,0,-fH,0).
Massive ; fracture conchoidaL H. =4' 6 to 6. Opaque ; resinous.
Bright yellow to reddish brown ; streak brownish yellow. B.B.
infusible, darkens with the heat ; colour restored on cooling. C.c:
ccrium 17'6, fluorine 10'9, sesquioxide of cerium 66'4, water 6'1.
From Finbo.
37. Bastnaesite, Ce,F,-f Ce,Oa-h4HjO, and
38. HAMAE'nTE,2(LaO,CeO)3CO,-hCeF^are similar. Thefirstia
from Baatnaes in Sweden, the second from Pike's Peak in Coloiada
384
MINERALOGY
Fig. 271.
Fig. 272 (species 42).
S9. Fldellite, AL,F,.
Right prismatic. In acute rhombic octahedrons with troncated
Spex. Polaredges 109°6' and SQ'IZ", middle 144°. H.-3. Laatro
ntroooB. Colour white; transparent Stenna-gwyn in Cornwall.
40. Cryolite, SNaF + AljF,.
Anorthic ; but mostly in cleav-
»ble masses. M:T 9V5T ; P:T
90° 2*; P:M 90° 40'. CI. P
perfect, U and T imperfect ;
brittle. H. - 2 -5 ; G. - 2 -9 to 3 03.
Vitreoaa, somewhat pearly on P.
Translucent ; after immersion in
water transparent. Colourless and
snow-white ; but when deep-seated
brown to black. Melts even in
flame of candle to a white enamel.
In open tube traces of hydrofluoric
ocid. Sol. in 8. acid. C.c: alumi-
nium 13, sodium 32-8, fluorine 54-2.
Arksutfiord, Greenland ; Miask,
Siberia. Used for manufacture of a white glass, and extraction of
clnmioium.
41. AEKStrriTK, (CaNa)jF-l-AL,F,. Ca:Na=-l:3.
Massive granular. H. -2-6; G. -3-03 to 3-18. CI. one distinct
Vitreous; whit«-{ translucent C.c: aluminium 18*6, sodium 23*3,
calcium 6-8, fluorine 61 'S. Arksutfiord.
42. Chiolite, 3NaF-l-2AljFs.
Pyramidal, and twins (fig. 272).
Middle edge 111° 14'. Mostly granu-
lar. CL imperfect. H.-4; 0.-284
to 2 '9, Resinous ; white. Fuses more
easily thau cryolite ; evolves hydro-
fluoric acid. C.c. : aluminium 186,
sodium 23 '4, fluorine 68. Ilmen
Uts. near Miask.
48. Chodneffite, 2NaF-fAIjF,.
G. -3. Other characters like chiolite, and from same locality.
44. PACHNOLfTE, 3(CaNa)F -h Al jF, -)- 2HjO . Ca:Na-3:2.
Oblique prismatic. ooP 98° 34'; always twins. Vitreous ; white ;
aemitransparent C.c. : aluminium 12'3, calcium 16'1, sodium 12'4,
Suorine 61 '1, water 8'1. Evolves water with crackling, when
heated ; other characters like cryolite, along with which it occurs in
Greenland.
45. TuoMSENOLiTE, 2(CaNa)F -H AljF,-H 2H,0 . Ca:Na-7:8.
Oblique prismatic. Prismatic planes striated; ooP 89° (fig. 273),
CI. basal, perfect. H. -2-5 to 4 ; G. -274 to2'76. Vitreous; cleav-
age face pearly. White with yellow crust; translu-
cent C.c: eluminium 15, calcium 16"4, sodium
7 -6, fluorine 52 '2, water 9-8. B. B. fuses more easily
than cryolite to clear glass, decrepitating violently.
Along with cryolite in Greenland.
46. GEARKStTTiTE, CaJF-l-Al3F3■^4HaO.
Earthy. H. =2. White; dull ; opaque- C.c:
aluminium 15"6, calcium 19*3, sodium 2*5, fluorine
41 ".2^ water 20 '3. Along with cryolite.
47. EviOTuKiTE, 2CaF5 + Al,jFe + 2H,0.
Crystalline. Soft ; brittl <; like kaolin. O.c. :
calcium 22-39, aluminium 16'23, sodium '43,
fluorine 65-24, water 5-71. Arksutfiord, Green- "i- -"3 (sp. 46).
bnd.
48. Pkosopite.
Oblique prismatic. A hydrated silico-fluorido
•f aluminium and calcium. H. — 4; G. — 2-89.
Colourless imbedded crystals. From the tin-
mines of Altcnberg.
49. Calomel, HgjCl.
Pyramidal ; P 136° 60' (fig. 274). H. -1 to 2 ;
O. — 6-4 to 6-5. Translucent ; adamantine. Yel-
lowish white to grey. Sublimes unchanged in closed
tube ; with soda yields mercury. InsoT. in n. acid.
C.C- : mercury 85, chlorine 16. Moschellnndsberg,
Jdria, Almaden.
50. SvLViTp, KCl:
Cubio (figs. 26, 30); also massive. CI. cubic.
•H. -2; G- 1-9 to 2. White or colourless. 97, ,„ ,r,.
Vitreous; soluble; taste like common salt "»■ ■"» W- '"'-
C.c: potassium 626, chlorine 47-5. li.B. fuses, and colours
flame violet. Crater of Vesuvius, and salt lieds of SUssfurt
61. Halite {Cmmium Salt, Rock-aalt), NaCl.
Cubic ffig.21) ; generally granular, sometimes fibrous. CI. cubic.
H. — 2; O. — 2'1 to 22. Transparent to translucent; vitreous
Colourless or white ; but often coloured red, yellow, or blue.
Taste saline. B. B. fuses and partly evaporates ; colours flame
yellow. C.C.I sodium 393, chlorine 607. In great bods «l
Wieliczka, Salzburg, Bex, tc, on the Continent; Cheshire ii
England. As an efflorescence in Brazil, Abyssinia, the Caspian and
Aral Seas. As a sublimation among lavas at Vesuvius and othef
volcanoes.
52. Salmi AC, NH^Cl.
Cubic (figs, 30, 40, and 41 with 26, S3, 40). CI. octahedral ; also
atalactitic, globular, and as an efflorescence. H. = 1 -5 to 2 ; G. — 1 '5
to 1 -6. Pellucid ; vitreous. Colourless, but sometimes stained.
Taste pungent. B.B. directly volatile ; in copper colours flame
blue-green. C.c. : 32 ammonia, 66-4 chlorine. A sublimate oi
active volcanoes. Vesuvius, island of Volcano, Iceland, Neai
coal-seams which have taken fire, in Scotland and at Newcastle,
53. Chloro-Calcite, CaCl-H(KCl, NaCl).
Cubic. Vesuvian bombs.
64. Cerakqteite, AgCl .
Cubic (fig. 26). Twins on octahedral face. No cL ; chiefly
massive in crusts. H. — 1 to 1'5 ; G. -=5-5 to 5-6. Fracture con.
choidal. Malleable. Translucent; adamantine to resinous. Grey,
yellowish, and greenish. B.B. fuses easily to a dark bead, reduced
m inner flame. Soluble in ammonia. C.c: silver 76, chlorine
26. Johann-Georgenstadt, ilexico, Pom.
65. Embolitf., 2AgBr-f3AgCT.
Cubic (fig. 29); also massive or concretionary, H. — ltol-6;
G. "5-8. Adamantine to resinous. Green and yellowish green,
C.c: silver 67, chlorine 13, bromine 20. Chili, Mexico, Honaoraa
56. Bromite, AgBr.
Cubic (figs. 26, SO). H. = 1 to 2; G. = 5 -8 to 6. Splendent Yellow
to olive-green ; streak siskin-green. B.B. fusible easily. Co.:
silver 57-5, bromine 42-5. San Onofre and Plateros (Mexico),.
67. Iodite, Agl .
'Hexagonal. CI. basal; also massive, and in crystalline plates
some inches in width ; these are flexible. H. — 1 to 1 '5 ; G. —
6'6to 5-7. Translucent ; adamantine- Citron and sulphur-yellow ;
streak yellow. B.B. fusible, colours the flame purple-red, and
leaves button of silver. C.c: silver 46, iodine 64. Zacatecas Ib
Mexico, Algodones in Chili Arizona, rarely in Spain.
68. COCCINITE, Hglj.
In grains of an adamantine lustre, from Casas-Viejas in Mexico,
Colour red to yellow ; in acute rhombic nrisms. Also from Zimapas
and Culebras.
69. TocoRNACLrre, AgI-(-Hg,I ,
Amorphous, yellow, soft. Chafiarcillo in ChilL
60. COTtTNNlTE, PbCl,
Ri^ht prismatic H. - 2 ; 0.-6 238. Transparent ; high ada-
mantine to pearly. White. Co.: lead 74, chlorine 26. Crater of
Vesuvius.
61. MoLTsrrr, Fe,Cl,.
Incrusting. Brownish red and yellow. On lavas of Vesuvius,
C.c: iron 34-5, chlorine 66-5.
62. Carnallite, KCl-^2MgCl-^]2HJO.
Right prismatic. Noel. Conchoidal fracture, H. — 2 to 2'6;
G. — 1-6. -Colourless, generally red from iron. C.c: 84 '2 chloride
of magnesium, 26 9 chloride of potassium, 38-9 water. Stassfurt,
Galicia, Persia.
63. Tachhydrite, CaCl-H2MgCl-f 12HjO.
Massive. Yellow, translucent, very deliquescent. In anhydrite.
C.c: calcium 7"46, magnesium 9-61, chlorine 40-34, water 42"69.
Stassfurt.
64. Kremersite, KCUNH.Cl-f Fe,Cl,-f3H,0.
Cubic ; in octahedra. Ruby-red. Soluble. Fnmaroles of
Vesuvius.
65. ERiTHROsiDEnn-E, 2KCl-fFe,Cl,-(-2H,0.
Righ t prismatic . Vcsm-ian lava,
66. Matlockite, PbCl-t-PbO.
Pyramidal; P 136° 17'. Crystals tabular. CL basal; fracture
conchoidal. H. -2-5; G. -7-21. Translucent; adamantine.
Yellowish white. B. B. fuses cosily with decrepitation ; coloura
flame blue. C.c: chloride of lead SDS. oxide of lead 44"6.
Ciomford in Derbyshire.
67. MENDiriTE, PbCl-H2PbO.
Right prismatic; chiefly massive CI. ooP perfect 102° 86'. H.-2-5
to 3; G. -7-to 7-1. Fracture conchoidal. Translucent; adaman-
tine to pearly. Yellowish or greyish white. BB. decrepitates, fuses
MINERALOGY
385
Fig. 276 (sp. 69).
«*oly. SoL in n. acid. C.c. : cUoride of lead 40, protoxide of
lead 60. Uendip Hills, and Brilon in YTeatphalia,
68. SOHWASTrEMBBEQITE, PbI+2PbO.
Bbombohedial ; in thin crusts. H. -2 to 2'5 ; G. -67 to 6'8.
Adamantine. Honey-yellow. Desert of Ata-
cama.
69. Ataoamitb, CnCld-3CaO,HjO.
Eight prismatic ; ooP (JO 112° 25', ?«> (P)
105° Iff, oof ao (A) (6g. 275); also reniform.
CL h perfect. Semitransparent ; vitreous.
Emerald - green ; streak apple-
green. B. B. fuses, leaving cop-
er. Easily soluble in acids.
!.c. : copper protoxide 55 "85,
copper I486, clilorine 16'61,
water 12 '68. Atacama, Cliili ;
Tarapaca, Peru ; Bolivia ; Burra-
Borra, Australia ; Serra de
Bembe, Ambriz, Airica ; Vesu-
Tius and (!) Etna.
70. Tallinoitk, Cua, HjO-UCqO, H,0.
In crusts. H. -3; G. -3-5. Bright blue to
greenish blue. Translucent : brittle. Botallack
in CornwalL
71. Pekctlite, (PbCl + PbOj-KCua-t-CuO).
Cubic (com. of figs. 26, 30, S3, 36). H.-2.
Vitreous. Sky-blue. Sonora in Mexico.
72. CoffKBLLITE.
rig. 276 (sp. 72). H^j^onaj (gg 276). b : r U3' IV ; r : r 132°
60*. Crystals acicular. Vitreous ; translucent. Vitriol-blue. A
chloride and sulphide of copper. Wheal Unity and Wheal Damsel
(Oomwall).
OXIDES OF METALS.
I. SlTBOXIDES XKD PBOTOZIDE.S.
73. CtJPEITK, CujO
Cubic (fies. 22, 30, 33, 26, with 39, 40). Compact and granular,
a. octohedral ; brittle. H. -3-5 to 4 ; G. -67 to 6. Transparent
and opaque ; adamantine. When transparent, crimson ; when
opaque, cochineal or brick-red. Often tarnished grey. B. B.
becomes black, fuses, and is reduced on charcoal. Soluble in acids
and in ammonia. C.c. : 88'9 copper, ll'l oxygen. Cornwall,
Siberia, Benat, Chessy near Lyons, Linares in Spain, Urals, South
Africa, BurraBorra. Valuable copper ore. ChaUxtrichiU consists
of cubes elongated so as to become fibrous. Tile-ore is a ferruginous
variety. Hepatic copper, liver ore, or pitchy copper ore seems to
be a product of the decomposition of chalcopyrite. DclafowiU,
Ca,0 -t- Fe,0, , from Bohemia and Siberia.
74. Watbb, H,0 .
Hexagonal, when solid, in complex twins in snow crystals;
rhombohedrio. by cleavage, in ice, H. — 1 '5; O. — •918. Hence 1000
of water— 1039 "5 of ice, or water expands I'l-th in freering. Trans-
parent ; vitreous. Colourless, but in bulk pale emerald-green. B
117° 23". CL basal Water when pure colourless, in mass bluish
green. Occurs in centre of geodes of chalcedony in China ; of
aruses of quartz in California and many other countries ; in
laolitic cavities to the amount of several gallons in the Faroes, also in
the Hebrides, &c Water of the ocean, from holding saline matters
in solution, has 0. — 1 027 to 1 0285. Waters of saline lakes contain
sometimes 26 per cent, of salts, and have G. 1'212. Besides its
vast bulk in the ocean, water occurs in enormous amount in the solid
form, often as water of crystallization in rocks and minerals, e.g.^
leolitea. Igneous rocks in some districts are converted largely
into saponite, which contains 25 per cent of water. Water is the
standard for specific gravities of solids and liquids ; 1 cubic inch
tX 60° F. and SO inches of the Wometer weighs 252'468 grains : 1
litre weighs 1000 grammes.
75. PSBICLASB, MgO.
Cnbic ; in cubes and octahedrons. CL do. H. — 6 ; G. — 3 '6 to
876. Transparent ; vitreous." Grey to dark greeiL B.B. infusible.
SoL in acids. C.c : magnesl*, with 6 to 8 of iron oxide. Somma.
76. BtnfSENiTE, NiO .
Cnbic ; in octahedrons. H. — 5'6: Q. — 6'4. Vitreous. Pistachio-
'green. Johann-Georgenstadt.
77. ZlKOITE, ZuO. _
Hexagonal and granular. CI. basaL H.-4 to 4'6 ; 0. -6'4 to
6*5. Adamantine ; translucent Blood- or hyacinth-red ; streak
.orange-yellow. B.B. infusible, but phosphoresces. C.c. : zinc
80 '26, oxygen 19 '74; sometimes with nianeanesa peroxide.
Valuable ore of zinc. Franklin and Sterling in New Jersey.
78. Massicot, PbO.
Massive ; scaly crystalline. H. — 2 ; G. — 7 '8 to 8. Sulphur- or
lemon-yellow ; often contains iron. Popocatepetl in Mexico.
79. Melaconite, CuO .
Cubic; compact H. -3 to 4; 0.-6 to 6 '3. Black. RB.
infusible ;.solu Die in acids. Cornwall, Leadhills, Lake Superior,
Burra- Surra.
80. Tenoeitk, CuO.
Oblique prismatic ; occurs in thin scales of metallic lustre on lava
of Vesuvius. Colour black and dark-red.
2. SEsqinozioEs.
81. COKUNDDM, AI5O,.
Hexagonal ; R 86° 4'. Twins common. CL rbombohedral, and
basaL Excessively tough, and difficultly frangible. H. — 9 ; G. — 3 'S
to 42. Transparent or translucent ; vitreous, but pearly to metallic
on basal face. B. B. unchanged. As Corundum, white, grey, and
greenish, frequently with bronzy lustre on basal face. C.c.: alumina,
with a little peroxide of iron. China, Ceylon, Bohemia, Malabar,
Macon in North Carolina (one crystal SOO lb weight). Emery ia
compact, crystalline, granular ; grey, to indigo-blue. Asia Minor,
Naxos, Spain, Greenland, America. Corundum is usf d when crushed
for cutting and polishing gems in China and India, emery in powder
for grinding. Alumina oc-
curs also in a purer state in
transparent crystals of vari-
ous tints of colour. When
red and of the colour of
pigeon's blood they are
termed RvMta ; these come
from Syriam in Pegu, Ava,
Ceylon, Bohemia, and near
Expailly. When 5 carats in
weight a ruby is twice the
value of a diamond of the
same size, when 10 carats
three times the value.
When blue the crystal is the
Sapphire, found chiefly in
Ceylon and Pegu ; when
green it is the Oriental
Emerald, when yellow the
Oriental Topaz, wljen purple the Oriental Amethyst, — the adjective
here distinguishing them from the true or occidental stones of the
same name. Other tints of colour also occur, but with the excep-
tion of the red and blue they are seldom pure or deep. The prism
when Out with a hemispherical dome sometimes displays a six-
rayed star, either of a bnght gold or a silvery white colour, upon a
freyish blue ground. These receive the name of Asteria Sapphire).
he same crystal frequently shows portions of even three diiferent
tints. When perfectly devoid of colour, they are called Wattr
Sapphiret; such are little inferior to the diamond in brilliancy,
but do not disperse rays of light to the same extent
82. HSMATITE, FCjOj.
Hexagonal and rbombohedral ; E 86°. Crystals rhombohedric,
firismatic, and tabular. Twins with axes parallel. CI. E, and basal ;
racture conchoidal; brittle. H. -5'5 to 6 '6; G. — 5'1 to 6 '3.
Opaque, but in thin laminee transparent and blood-red. Brilliant
metallic lustre, iron-black to steel-grey, often brilliantly tarnished oS
red, yellow, green, and blue tints ;
streak cherry-red. B. B. in the inner
flame becomes black and magnetic.
Sol. in acids. C.c: iron 70, oxygen
30. The following are varieties or
subdivisions: —
Elba Iron Ore, highly modified
rhombohedtal crystals, often bril-
liantly tarnished. Specular Iron Ore,
in thin flat crystals, often from
volcanoes, as on the island 9f Ascen-
sion ; this variety includes Micaceous
Iron, thin, lamellar, and curved, and
Red Iron Froth, scaly. Red Heema-
tite, in botryoidal and stalactitic
forms, which are internally com- p^ ggo.
rosed of radiating fibres, and often t." j u
ave a concentric structure ; the external surface has a dark
red to a brownish red hue. Compact and Ochrcy varieties with
more or less aluminous impurity, pass into Reddle or red chalk, and
when still mnre earthy into jaspcry and columnar ores. This ore is
very commonly distributed:— micaceous iron at Pitficbie in Aberdeen
and Birnam in Perthshire ; red hxmatiu at LeadhiUs and at
XVI. — 49
Fig. 277.
Fig. 273.
386
MINERALOGY
tJlverston in LancasUrs ; specular iron at Taratock in Devonshire
and in Cumberland. Martite seems to be the same substance in
pseudomorpha after magnetite ; it occurs in cctahedra in Bute,
Framont (Vosges), New York, and BraziL
83. Ilmenite, (Fe,Ti).pj.
Rhombohedral ; R 86°. Ciystala rhombohedral and tabular, also
in twins. t'L basal ; fractuie conchoidaL H. — 6 to 6 ; G. — 4 '66 to 6.
Opaque, semimetallic, iron-black
to dark brown ; streak bJack or
reddish brown. Sometimes slightly
magnetic. B.B. infusible, but with
microcoimic salt forms a red glass.
Slowly sol. in s. acid when pow-
dered. C. c . : peroxide of iron, with
from 8 to £3 per cent oxide of
titanium. Occurs in metamor-
phic rocks. Common in chloritic -^S- 281.
gneiss in Scotland ; Menaccan (Cornwall), Ilmen Mountains, Salz-
burg, Egersund (Norway), Arendal, Dauphin^ (Crichloniie), Massa-
ohusetts ( Washin^ioniU).
84. LSEEINE.
Cubic ; in octahedra. Strongly magnetic ; in other respects similar
to ilmenite, but occurs in igneous rocks. Common as black iron-
sand in Scotland ; Iserweise in Bohemia, Auvergne, Canada, New
Zealand.
8. COMPODTTDS OF SeSQUIOXIBES WITH PROTOXIDES (SpHTELe).
85. MAONETrTE, FeO, Fe^Oj.
Cubic (figs. 35, 30, 33, 29, 34, 37, with 40, 41, 36). Hemi-
tropes common on octahedral face (fig. 169). Twins (fig. 261). Faces
of ooO striated in long diagonal. Often compact and granular. CI.
octahedral; fracture conchoidal or uneven ; brittle. H. »5'5to6-5;
G='4*9 to 5'2. Opaque; lustre metallic. Iron-black to brown;
streak black. Highly magnetic ; often polar, forming natural
magnets. B. B. beconies brown and non-magnetic, fusing with
difficulty. Powder sol. in h. acid. C.c. : 31 protoxide and 69 per-
oxide of iron; or 72 •4_ iron, 27 '6 oxygen; sometimes with titanic acid.
tn crystals in Shetland and Sutherland ; also Cornwall and Antrim,
Traversella (Piedmont), Tyrol, Styria. Massive atDannemora and
Taberg (Sweden), Norway, Urals, Harz, Saxony, Elba. This is
the most important ore in Norway, Sweden, and Russia, and affords
the finest iron.
86. Maonesio-Fekkite, MgO, FcjO,.
Cubic (fig. 30). H. "6 to 6-5; G. =4-57 to 4-66. Other
;haracters same as magnetite. C. c. : magnesia 20, peroxide of iron
S7. Fumaroles of Vesuvius.
87. Jacobsite, (MnO, MgO), (FcjOj, Mn^Oj).
Cubic ; O. Black ; vitreous ; streak red. Nordmark in Sweden.
88. FEANKLtxiTE, (FoO, ZnO , MnO), (FejO,, Mn^Oj).
Cubic (figs. 34, 64) ; also granular. CI. octahedral ; fracture
conchoidal ; brittle. H. =5-5 to 6-5 ; G. -5-07. Metallic lustre.
Iron-black ; streak reddish brown. Opaque ; slightly magnetic.
B. B. infusible, but shines and throws out sparks. On charcoal with
soda a deposit of oxide of zinc. Sol. in h. acid with evolution of
chlorine. C.c. : about 67 iron oxide, 17 manganese peroxide, 16
zinc ox-ide. Franklin and Sterling (New Jersey).
89. CnitOMiTE, FeO, CrjO, .
Cubic ; in octahedra, generally grannlar-massive. H. = 5 "5 ;
G. — 4 "4 to 4 '6. Opaque ; semimetallic to resinous. Iron-black to
dark brown ; streak reddish brown. Fracture uneven ; sometimes
magnetic. B. B. unchanged ; in red. flame becomes magnetic; with
borax forms an emerald-green bead. Not soluble in acids. C.c:
19 to 37 protoxide of iron, 0 to 15 magnesia, 36 to 64 peroxide of
chromium, 9 to 21 alumina. Unst (Shetland), Towanrieff (Aber-
deenshire), Silesia, Bohemia, Styria, Urals, Turkey, Baltimore,
Massachusetts, and Hoboken. The ore of chromium ; used for
dyes. Irite is chromite mixed with iridosmium.
90. UriANiNiTE {Pitch BUndt), UO, U5O3.
Cubic (fig. 30); usually massive and botryoidal. H. -5 to 6;
G-6-5to8. Lustre pitch-like to submetallic. Colour velvet-black,
brownish black, and grey. B.B. infusible. Not sol. in h. acid,
but easily in hotn, acid. C.c. : oxides of uranium 80, with a mixture
•f other oxides. Jobann-Gcorgenstadt, Annaberg, Przibram, Red-
roth in Cornwall. The chief ore of uranium.
91. Gahnite, ZnO, k\0,.
Cubic (figs. 166, 30, 33, and with 39, 40). Hemitropes like
magnetite. CL 0; brittle, with conchoidal fracture. H. -7'5to
3 ; G. —4 '3 to 4 '9. Opaque; vitreous to resinous. Dark leek-green
to blue; streak grey. B.B. unchanged. Unafi"ectcd by a* ids or
alkalies. _ C.c: 44 oxide of zinc, 66 alumina. Falun, Broddbo,
Iladdam in Connecticut, and Franklin in Now Jersey. DysluiU:
c^ntiins 42 per cent, sesquioxide of iron; and KrciUonite contains
24 .j.Tide of manganese.
92. Heeotnite, FeO, Al,Ot.
Cubic; generally granular massive. H. "T'B to 8; G>— S'tto
395. B.B. infusible. C.c. : oxide of iron 41 1, alumina 68"9.
Ronsberg in the Bohmerwald.
93. Spinel, MgO, AIJO,.
Cubic (figs. 30, 33, 40with26); henutropeetmitedbyfaceof 0. CL
octahedral ; fracture conchoid.1l. H. — 8 ; G. — 3 "4 to 4 •!. Trans-
parent to opaque ; vitreous. Black, red, blue, green ; streak white.
B.B. infusible and unchanged. C.c: 28 magnesia, 72 alumina;
some with a little iron, and the red varieties some chromium.
Varieties are — Spinel Rvjby when Ecarlet, £alas Buhy when rose-red ;
both often sold as the true ruby, but not nearly so valuable ; whem
of 4 carats valued at half the price of a diamond the same size. These
Fig. 282.
Fig. 283.
come from Pegu (native name Balachan). The violet-colonred_is the
Alabandinc r«6y from Alabandin in Caria, (Asia Minor). The orange
red is the RuliuUa. The above also occur at Ceylon, Ava, and Slam.
Sapphirine is pale sapphire-blue to greenish or
reddisli blue ; from Akcr in Sweden, Greenland,
and North America. Plamastc, dark gi'een or
blue to black; from Candy in Ceylon. Chloro-
spiiicl, grass-green with a yellowish white
streak ; from Zlatoust. TVaUr-spincl colour-
less ; from Ceylon. Picoliie is a dark blue
chromiferous variety from serpentine.
94. Cheysoeektl, GIO, AljOj.
Right prismatic (fig. 284). Twins common,
united by a face of Pco (fig. 285, also 156). CI.
brachydiagonal imperfect, macrodiagonal more
so ; fracture conchoidal. H. - 8 -5 ; G. - 3 68 to
3 8. Transparent or translucent ; vitreous.
Greenish white, leek-green, and dark emerald- ^'^- 284 (sp. M).
green. B.B. infusible. Not affected by acids.
C.c: glucina20, alumina 80. Brazil, Ceylon,
India, the Urals, Haddam in Connecticut. A
very valuable gem. It sometimes possesses an
opalescent band, which when the stone is cut
en cahochon appears as a streak of floating
light ; whence it derives its name of Cymo-
phane. It is then also called the chatoyant or
Oriental chrysolite, and when fine is of extreme
value. The emerald-green variety, or Al<x-
andrile, is columbine-red by transmitted light.
Fig. 286.
4. Dectoxides.
6. RTmi.E, TiOj.
Pyramidal ; prisms dominant. P 84 40'; Poe
65* 85' (figs. 286,
th axes of halves 114° 26'. CL
H. ~6 to 6-6; G. -4-2 to 4-3. Tr«ns-
287). Hemitropes
00 P and 00 Pco , perfect,
parent to opaque ;
adamantine lustre.
Brown-red, red, pale
yellow, and black ;
streak yellowish brown.
B. B. unchanged ; with
borax in the ox. flame
forms a greenish, in
the red. flame a violet
glass. Not affected by
acids. C.c; titanic
acid, with some per-
oxide of iron. Craig-
cailleach and Bon-y-
Gloe (Perthshire), The „ „., _., „™
Cobblcr and Ben-Bheula ^- 288- ^ig- 287.
(Argyllshire), Alps, Limoges, Norway, Brazil. Large crystals at
Titanium Mount (Lincoln county, Georgia). Used in porcelain
painting, and for tinting artificial teeth. When attenuated cryntaU
arc imbedded iu tvck-crystai they are called Vcnua' hair.
MINERALOGY
387
96. AnkTABT, TiO,.
Pyiamidal ; pyramids dominant P IM* S6' (fig. 288). CL
Wjal, and P, both perfect j brittle. — —
lL—&'6 to 6; G. -Is -8 to 3-93. Tnui8-
uannt to opaque ; lostre adamantine to
metalUo. lidigo-blae, yellow, brown,
rarely colonrless ; streak white. B. B.
iofiisibla. SoL in hot b. acid. C.c. :
titanic acid, with a little iron and rarely
tin. Cornwall and Devonahire, the Alps,
'Janphin^, Valaia, the UnJa, Minaa
Ueraea (Brazil).
97. Beookitb, TiO,.
Right prismatic ; with polar edges 136°
37' and 101° 8' (fig. 289). CI. macrodia-
gonaL H.-5-6 to6; 0.-3-86to4-2.
Transparent to opaque ; lustre metaUic "B- 288 (ep. 96).
adamantine. Yellowiah, reddish, and hair-brown; streak yellowish
white to white. B.B. infusible; with
microcosmic salt, a brownish yellow
glass. C.c. : titanic acid, with 1 to 4 6
per cent, peroxide of iron. Snowdon
and Tremadoc ("Wales), Chamouni,
Bourg d'Oisans, Miask. Arka-nsiU is
iron.black, and submetallic, in thick
crystals from Arkansas, U.S.
98. Caksiteeitb, SnO,.
PyramidaL P 87° 7'; P«> 67° SO*
(figs. 290 to 292). Crystals ooP, P;
or ooP (j), P (s), o.Poo(0; or with Poo
(P), (fig. 290); and also ooP2 (r), and
SPJ (z), (fig. 291). Hemitropes very
common, combined by a face of Poo with
thechief axes 112° 10' (figs. 293, 171, 172, 173); also fibrous ( JTooi
Tin), or in rounded fragments and grains {Stream Tin). CL pris-
nstie along ooP, andooPoo, imperfect; brittle. H. — 6 to 7;
^ Kg. 289 (sp. 97).
I «[• * l!;*:rrj|s
ill ' )-^-— *. I
Fig. 29a
Fig. 291.
O.— 6'8 to 7. Translucent or opaque; adamantine or resinous.
White, but usually grey, yellow, red, brown, and black ; streak
white ''"ht gie- or brown. B.B. in the forceps infusible ; on
Pig. 292.
Fig. 293.
charcoEkL, in the inner flame, reduced to tin. Not afi°ecte£ by acids.
C.c: 78 '6 tin and 21*4 oxygen, but often mixed With peroxide oi
iron, or manganese, or tantalic acid. Cornwall, Bobe^iia, Saxony,
also Silesia, Haute-Vicnne in France, Greenland, Russia, North
and South America, Malacca, Bancs, and Queensland. Almost
the only ore of tin.
, 99. Hacsmaknite, 2iln0, llnO,.
Pyramidal. P 116° 59'; Poo 98° 32' (fig. 110). Twins common,
and rosettes of twins (fig&..174, 175). CI. basal, perfect, less so P and
Pco ; fracture oneveo. H. — 6'5 ; Q. — 4°7 to 4'8. Opaque; metallic
butie. Iron-black; streak brown. B.B. infusible, but becomes
orcomjMt
brown. Sol. in h. acid, with eTolution of chlorine. Powder coionra
8. acid red. C.c. : 31 protoxide and 69 perozids of manganese.
IhleTeld and Ilmenau in the Earz, and Sweden.
100. Bravtnite, MnO, MnO,.
Tetragonal, P 108'^39'. CL P ; brittle. H.-6 to6-6 ; G.»47 to
4'9. Metallic lustre. Coloor and streak dark brownish black.
Co.: 70 manganese and 30 oxygen, generally with about 8 percent,
of silica. Ihlefeld and St MarceL Uarceline has violet tarnish.
101. Pteolusite, MnO, .
Right prismatic; oe>P93°40';
earthy. CI. o=P ; friable. ff.-2to2-6;
G. =-47 to 5. Opaque; lustre silky to
send-motallic Dark steel-grey to black ;
streak black. Soils. B.B. infusible, loses
oxygen and becomes brown. SoL in h. acid,
with evolution of chlorine. C.c: manga-
nese 63, oxygen 37. Amdilly (Banffshire),
Cornwall and Devon, Ilmenau, Ihlefeld,
France, Hungary, Brazil. Used for n
moving the green iron tint from glass ; hence
its name and that of Savon de verrUr. Also
for obtaining oxygen and chlorine. Vdr-
viciu is a variety with 6 per cent, of water,
from Warwickshire.
Fig. 294.
102. CREDNEBrrE, 3CuO, 2(MnO,MnO,).
Oblique. H. -4'6; G-E. Metallia Black; streak brown.
Thuringia.
103. PU.TTNEEITB, PbO,.
Hexagonal. oc.P120°. CL indistinct ; brittle. G. -9'4. Opaqnef
metallic. Iron-black ; streak brown. C.c : lead ii% oxygen
13-8. Leadhills.
104. Mnmra, 2PbO, PbO,.
Pulverulent H. = 2 to 3 ; G. - 4 -6. Dull. Colour bright red ;
streak orange-yellow. B. B. fuses easily and reduced. SoL in h.
acid. C.c : lead 907, oxygen 93. Leadhills, Weardale in York-
shire, Anglesea, Badenweiler, Siberia.
S. Hysbocs Oxides.
106. Sassoline, BjO, , H,0 .
Anorthic OP : oo?oo 75° SO'. Scaly six-sided plates. CS.
basaL Flexible and sectile. H. — 1; G. — 1'4 to 1'6. 'Translucent;
pearly; white; taste bitter; greasy. SoL in hot water. C.o.i
Doracic acid 56 '46, water 43 '55. Hot springs of Sasso, near
Siena, Tuscany; and with snlphor in the crater of Volcano,
Lipari Islands.
106. TtTBGiTE, 2Fe20,-HH,0.
Massive and fibrous, also earthy. H."-6to6; G. — 3'64 to 4'68.
Lustre satin-like, also dulL Colour reddish black to bright t«d.
Botryoidal surfaces lustrous like limonite.
Opaque. C.c : iron sesquioxide 947, water /^j_ ' /^Vv
5 3. B.B. decrepitates violenUy and yields /^ ""^^^v
water. ■ Kerrera (Hebrides),
(Urals), and many limonite localities. Fre-
quentiy taken for limonite.
107. DiABPOBE, A1,0,, H,0.
Right prismatic; a>P129°47'; usually thin
foliated. CL brachydiagonal, perfect ; brittie.
H.-6;G.-3-3 to 3-4. Vitreous; pearly on
cleavage-planes. Colourless to yellowish,
greenish, or violet. B.B. infusible, decrepi-
tates. Insoluble. C.c. : alumina 85, water
f ^
Fig. 296 (sp. 1C7).
Schemnitz, Broddb' Switzerland, Nazos, Chester, Massa-
chusettB. Fig. 295.
108. OSTEITE, Fe,0,, HjO.
Right prismatic ; ooP 94° 63' ;
also columnar, fibrous, or scaly.
CL brachydiagonal, perfect ; brit-
tle. H.-5to6-5; G.-.3-8 to4-4.
Opaque ; or fine crystals trans-
parent, and hyacinth-red ; lustre
adamantine or silky. Colour
yellow, red, or dark brown ; streak
brownish yellow. B.B. becomes
magnetic, difficultly fusible. SoL
in n. acid. C.c. : peroxide of
iron 90, water 10. Hoy (Orkney),
Achavarasdale (Caithness), Salis- -i^g. 296. Fig. 297.
bury Crags (Edinburgh), Lost- „ .v
withiel, CUfton, BristoL Praibram, Siegen, Saxony, Urals, NortH
America.
388"
MINEKALOGY
109. Manoanitb, MD.O3 , H,0 .
Right prismatic, sometimes liemihedrio ; ooP {M) 99 '40.
prismatic (figs. 293 to 300); vertically striated;
also columnar or 6brou8. Hemitropea cora-
mon. CL brachydiagonal, perfect; brittle.
H.-S-5 to 4; G.=4-3 to 44. Opaque;
metallic lustre. Steel-grey to iron-black;
streak brown. B. B. infusible. Sol. in warm
h, acid. C.c. : peroxide of manganese 89*9,
water lO'l. Grandholm (Aberdeenshire),
Cork, Upton Pyno (Exeter), Churchhill
(Somerset), Warwickshire, Ihlefeld, Thuringia,
Norway, Sweden, Nova Scotia.
Fig. 299 (sp. 109).
110. LtMONiTE, 2Fe,Oj+3HjO.
Fibrous, bottyoidal, and stalactitio, some. i,. ,,f,n-r ,r,n>
times earthy. H.-4-5 to 5 -5; G.-3-4 to ^'S' -iOO (^P- 109)-
3*95. Opaqne ; lustre silky, glimmering, or dull. Brown, yellow-
ish and blackish brown, often black on surface; streak ochre-
yellow. In closed tuba yields water and becomes i-ed. B.B. in
inner flame becomes magnetic, fusing to a glass. C.c. : peroxide
of ii-on 85-6, water 14-4. Sandlodge (Shetland), Hoy (Orkney),
Clifton, Bristol, Cornwall, Harz, Thuringia, Nassau, Styria, Carm-
thia, Siberia, United Stater
111. Xanthosideeite, FejOj, 2HjO.
Fibrous, Btellate, also aa an ochre. H. --2'5. Siliy or greasy,
pitch-like or earthy. In needles, golden-yellow or brown-red; as
an ochre, yellow, red, or brown; streak ochre-yellow. B.B. like
limonito. C.c: peroxide of ironSl '6, water 18-4. Hoy(Orkney),
Achavaxaadale, Kilbride, Wioklow, Ilmenan, Goslar, andElbingerode
in the Harz.
112. Beauxite, (3AIj03, Fifi^), 2HaO.
Oolitic, concretionary, disseminated ; also earthy and clay-like.
G. -2'56. JVlite, grey, ochre-yellow, brown, and red. C.c:
alnmina 50 '4, peroxide of iron 26-1, water 23-5. From Beaux (or
Banx) near Aries, and elsewhere in France. In grains in compact
limestone. Pore varieties used for manufacture of aluminium.
113. KilAfliTE, Us03-l-2H30.
Amorphous masses; resin-like. H. — 3'5 to 4 '6.; G. — 4 to 5.
Reddish brown to black ; streak wax -yellow to olive-green. C. c. ;
68 '5 percent, sesquioxide of uranium, 10 of water, with impurities.
Elias mine (near Joachimsthal).
114. Bruoite, MgO,H.O.
Rhombohodral ; R82°22'; also foliated and botryoidal columnar.
CI. basal, perfect ; sectile ; laminte flexible. H.— 2;G. — 2'3to2'4.
Translucent, pearly. Colourless. B.B. infusible. Easily soluble in
acids. C.c : 69 magnesia, 31 water. Nemalite is a fibrous variety
with silky lustre. Swinaness and Quin Gio in Unst, Beresovsk
in the Urals, Hoboken, New Jersey, Texas, Pennsylvania.
115. PrKOCHKOiTE, MnO, HjO.
Foliated. H. -2-5. Pearly, white, but changing through bronze
to black. Flesh-red by transmitted light. In matrass becomes
virdigris-greon, finally black, yielding water. SoL in h. acid.
C.c. : protoxide of manganese 79 '8, water 20 -2. In veins in mag-
netite at Paisberg in Sweden.
116. GiBBSITE (HydrargiltUe), Al.Oa, SIIjO.
Hexagonal. C.c: 65-5 .ilumina, 34-5 water. The crystals are
from Zlatoust in the Urals ; stalactites from Richmond in Massachu-
setts and Yilla Rica in Brazil.
117. LiMNITE, FojO,, 3II3O.
Massive in stalactites, also as a yellow ochre. Like limonite, but
pitchy lustre. C.c. : peroxide of iron 74 '8, water 25"2. Lcadhills,
Botallaok (ComwaH),. Novgorod (Russia).
il8. nrBROTXloiTe^mjUjt.ffifjO-f OMgO, HjO-fSHjv,
Hexagonal.'ACl; basal; foliated, and somewhat fibrous. H. - 2 ;
G. — 2"04. White, pearly. Greasy to the touch. Translucent.
0.0. : alumina 16'8, magnesia S9'2, water 44. . Zlatoust, Urals;
Snariun, Notwo-' • New York.
il9. PrsoAtmiTE, re„03, 3HjO-f 6MgO, 'B.^O-i-^VlJi.
Hexagonal ; tables and scaly coatings. Lustre pearly* to aoW
metallic Colour white to ^old-yellow. Translucent. B.B. im-
fusible, yields water. SoL in h. acid. C.c. : peroxide of van
23-9, magnesia 35-8, water 40-3. Haaf Gninay in Shetland, lAng-
ban in Wermland.
120. GCMMITE, UjOj, 3H2O.
In rounded lumps, resembling gum. H. —2*5 to 3 ; G. — 8*9 to
4 '2. Lustre greasy. Reddish yellow to yellowish brown. Co.: 71
per cent, sesquioxide of uranium water 14*75, with imT)uritiea.
Johann-Georgenstadt.
121. PsiLOMELANE, (BaO, MnO) MnOj-fSHjO, MnOj-f 3HjO.
Massive and botryoidal ; fracture conchoidal. H. = 5 *6 to 6 ; G, —
4-1 to 4 '3. Bluish black. B.B. infusible. About 80 per cent, of
oxide of manganese, with baryta, potash, and water. Hoy (Orkney),
Lcadhills, Cornwall, Devon, Schneeberg, Ilmenau, Vermont in
France. TVad is similar, but sometimes soft and light. Lcad-
hills, CJomwall, Harz, France.
122. Chalcophanite, MnOZnO-^-2Mn03-^2HJO.
HexagonaL R:R114'' 30'. G. basal' H. -2*6; G. -3*91.
Metallic lustre. Blue-black ; streak brown, dull. Opaque ; flexible.
C.c: manganese binoxido 5994, protoxide 6*6. zinc oxide 21*7,
water 11*6. Sterling Hill (New Jersey'
OXIDES OF NON-METALS.
1. OirDES OF Absenio-Antimont Family (TBEoxrois).^
123. Aksenolite, AsOj.
Cubic; in octahedra; also botryoidal, stalactitic ' H. — 1*6; O."-*
3*7. Lustre vitreous. White; streak pale yellow. Translucent'
Sublimes in closed tube, condensing in brilUant octahedra. C.0.1
arsenic 75*76, oxygen 24*24. Cornwall, Andreasberg, JoachimsthaJ.
Kapnik (Hungary), Nevada, California.
124. SENAKMONTrrE, SbOj.
Cubic ; in octahedrons. CI. octahedral, also massive granulAr.
H.-2to2*5; G. — 5*22 to5*3. Transparent; adamantine. WhiteM*
gi*ey. B. B. in inner flame fuses and colours the flame greenish bine.
Sol. in h. acid. C.c: antimony 83*56, oxygen 16*44. Endellioa in
Cornwall, Constantine in Algeria, Malaczka in Hungary.
125. Vaientineitb, SbOj.
Right prismatic; ooP 137'. CI. odP, perfect H. -2*6 to 3; G. -6*5
to 5 '6. Translucent; adamantine to pearly. Yellowish white, brown-
grey; streak white. Other properties and composition like senar-
montite. Glendinning (Dumfriesshire), Przibram, Bramifidorf
(Saxony), Harz, Hungary, Allemont (Dauphin^), Siberia.
126. Bismite, BiOj.
Massive, earthy. G. — 4*36. Grey, yellow, green. C.c:bismDtli
89*66, oxygen 10*35. St Agnes (Cornwall), Schneeberg, Siberia.
127. MOLiBDITE, MoOj.
Right prismatic; (»P136"48'. Incapillary crystals, also powfleiy.
-H. — 1 to 2; G. — 4*5. Straw-yellow to yellowish white. Co.:
molybdenum 65*71, oxygen 34*29. With molybdenite at maajr
of its localities.
128. TiruosTiTE, WO3.
Earthy. Soft yellow or yellowish green. Sol. in alkalies. C.c ;
tungsten 79*3, oxygen 20*7. Cumberland and Cornwall,- Monroe
in Connecticut
129. Cervantite, SbOj-fSbOj.
Right prismatic. Acicular, generallyearthy. H. — 4 to 6; G. — 4*1.
Isabel-yellow, reddish white. B.B. on charcoal reduced; xm-
alteredjiKr sf. Sol. in h. acid. Harehill, Ayrshire; Endellion, &c,
Cornwall ; Cervantes, Spain ; Felsbbanya, Hungary ; Mexico ;
Canada ; California.
130. STiBicoxrTE, SbOj, H3O.
Massive, powdery. H. -4 to 5*6; G. -5*28. Pale yellow.T In
closed tube yields water. C.c : antimony 74*9, oxygen 19*6, inter
6*5. Goldkronach (Bavaria)
131. ToLGEBrrE, SbO,, 5H3O.
Massive and iwwdcry. AVliite. In tube yields water, below red-
ness. C.c: antimony 53*9, oxygen 19*3, water 21*8. Constantine
in Algeria.
132. ZuimEREEZ {Tinder Ore).
In soft, flexible, tinJer-like masses. Colour dark cherry-red to
blackish red ; lustre glimmering. Two varieties : — one, from Klaus-
thai, contains antimony oxide 33, iron oxide 40, lead 16, sulphur 4;
the other, from Andreasberg and Ivlausthal, seems to be a n)ixturB
of jaracsonito (82*04 per cent.), mispickel (13*46), aud pyiarg}*rit«
(4*34)
133. Tellcriti.
YiUowibh or whitish. Radi.iled, spherical masses. Gives th«
reactions of tellurous acid. Facscbiiva and Zalathna, Colorado.
MINERALOGY
389'
134. TiJiTALIO OCBRE.
Powdery; brown; vitreous. Pennikoji in Finland.
2. Oxides of Cabbok-Silicos Familt (Bihoxidss).
186. QDAIII2, SiO,.
Hexagonal ; the pnrest varieties tatariohedral. The primary
prn:mi5 P has the middle edge -103° 34', and the polar edges -
Fig. 307. Fig. 308.
Fig. 301. Fig. 302. Fig. 303. Fig. 804. Fig. 305.
133° 44', and is often perfect. Very frequently it appears
as a rhombohedron B (or ^P), with polar edges— 91 16'.
Crystals often of o>P, P
or <x.P, P, 4P, the forms
ooP and 4P being combined
in an oscillatory manner,
producing strise on the face
of the prism (figs. 803, 304,
805); also ooP, P, J(2P2),
the last face appearing as a
rhomb replacing the alter-
nate angles between the two
other forms (figs. 307, 308).
They are prismatic, or py- Fig. 306.
nunidal, or rhombohedral,
when P is divided into R and -E; the latter
rery often wanting. Many faces plagihedral, as
in figs. 302, 306, 309.
Twins common, with parallel ares, and either
merely in juitaposition (see fig. 178) or interpene-
trating. Crystals often distorted, as in figs. 310
to 313. The crystals occur either single, attached,
or imbedded, or in groups and druses. Most frS:
nuently granidar, massive, fibrous, or columnar;
aUo in pseudoraorphs, petrifactious, and other
forms. CL rhombohedral along R, very imper-
feet; prismatic along ooP, still more imperfect;
fracture conchoidal, uneven, or splintery. H. — 7 ;
G. — 2o to 28; 2 65 in the pnrest varieties.
Colourless, but more often white, grey, yellow,
brown, red, blue, green, or even black. Lustre
vitreous, inclining to resinous; transparent or
translucent ; when impure almost opaque. B. B.
infusible alone; with soda effervesces, and melts
into a clear glass. Insoluble in acids, except the hydrofluoric
when pulverized, slightly soluble in solution of potash. C.c.
Fig. 309.
Fig. 310. Fig. 311. Fig. 312. Fig. 313.
48*05 silicon and 61 '95 oxygen; but frequently a small amount of
tho oxides of iron or titanium, of lune, alumina, and other
substances.
The following are varieties : —
llocicrystai : highly transparent and colourless ; Dauphin^,
Switzerland, "ryrol, Hungary, Madagascar, and Ceylon.
Amethyst : violet-blue (from iron peroxide or manganese), and
often marked by zigzag or undulating lines, and the colour dis-
posed in clouds ; Siberia, Persia, India, Ceylon, Brazil (white or
yellow, named false topaz), Hungary, Ireland (near Cork), and
Aberdeenshire. Wine-yellow (Cilrin and Gold Topaz) ; the brown
or Smoky Quartz (coloured by a substance -containing carbon
and nitrogen); and the black or iforion, from Siberia, Bohemia,
Pennsylvania, and other places. Cairngorm Stone, black, brown, or
•yellow, from Aberdeenshire mountains. The above are valued as
omunental stones ; those which follow are less so.
Base Quartz : red inclining to violet-blue; Clashnares Hill (Aber-
deen), and Rabenstein in Bavaria. UUk Quartz : milk-white, and
tUj^tly opalescent; Greenland. Prase: leek and other shades of
green; Saxony and Cedar Mountain in South Africa. Cafs-cye,.
inclosing asbestos: greenish white or grey, olive-green, red, brown,
or yellow ; Ceylon and Malabar. AvaniuriTiCf enclosing mica :
yellow, red, green, or brown; India, Spain, and Scotland. Sidtrite-^
indigo or Berlin blue ; Golling in Salzburg.
Common Quartz, crystallized or massive, white or grey, also red,
brown, &c., is a frequent constituent in mauy rocks. Some impure
varieties are properly rocks, as: —
(1) Ferruginous Quartz, or Iron Flint : red, yellow, or brown ;.
often associated with iron ores.
(2) Jasper : red, yellow, brown, also green, grey, white, and
black ; alone, or in spots, veins, and bands {Ribbon or Egyptian
Jasper) ; UraLs, Tuscan Apennines, Harz, and many parts of Scotland.
(3) Lydian Stone, or Flinty Slate : black, grey, or white ; has a
splintery or conchoidal fracture, breaks into irregular fragments,
and passes by many transitions into clay-slate, of which it is often
merely an altered portion, as in Scotland; used as a touchstone for
gold, and at Elfdal (Sweden) manufactured into omattents.
(4) ffomstone or Chert : compact, conchoidal, splintery fracture ;
translucent on the edges; dirty grey, red, yellow, green, or brown;
passes into flinty slate or common quartz; common in the Mountain
limestone. Oolite, and Greensand formations; and often contains
petrifactions, as shells, corals, and wood.
Other siliceous minerals seem intimate mixtures of quartz and
opal, as: —
Flint : greyish white, grey, or greyish black, also yellow, red,
or brown ; sometimes in clonds, spots, or stripes ; semitrans-
parent; lustre dull; fracture flat conchoidal; occurs chiefly in the
Chalk formation, as in England, Ireland, Aberdeenshire, France,
Germany, and other countries; sometimes in beds or vertical veins,
often in irregular lumps or concretions, inclosing petrifactions, as
sponges, echinoids, shells, or siliceous Infusoria. 'The colour is
partly derived from carbon, or organic matter. Used formerly for
gun-flints, and still for the maniuacture of glass and pottery; and
Cut into cameos or other ornaments.
Chalcedony : semitransparent or translucent ; white, grey, blue,
green, yellow, or brown; stalactitic, reniform, or botiyoidal, and
in pseudomorphs or petrifactions ; Iceland, Faroes, Trevascus in
Cornwall, Scotland, Hungary, Bohemia, Oberstein. Camelian:
chiefly blood-red, but also yellow, brown, or almost black ; India,
Arabia, Surinam, and Siberia; also Bohemia, Saxony, and Scotland
(Fifeshire). Plasvia: leek- or grass-green, and waxy lustre; Olym-
pus, Black Forest, India, and China.
Chrysoprase: apple-green; Silesia, and Vermont in NorthAmerica.
Moss-Agate and Bdiotrope : dark green and dendritic (called Blood-
stone when sprinkled with deep red spots) ; India, Siberia, Bohemia,
Fass^ Valley, island of Bum and other parts of Scotland.
136. Tridymite, SiO, .
Hexagonal ; P middle edge 124° 4', polar edges 127° 35'. Single
crystals, very minute hexagonal tables of OP, ooP, but with tno
eiga replaeed by P and ooP2. are rare (fig. 814). Mostly twinned
Fig. 314.
Fig. 816. Fig. 316.
in double or (oftener) triple combinations (figs.
315 to 317). CI. basal, indistinct; fracture con-
choidal. H. - 7 ; G. - 2 -282 to 2 -326. Colourless
and transparent; vitreous, pearly on the base. Fjg. 317,
B.B. like quartz. Co.; 90 silica, with some
alumina, magnesia, and iron peroxide, probably from the matrix.
Discovered by Von Rath in the trachyte of San Cristobal, near
Pachnca, in Mexico ; also in the trachyte of Mout-Dore (Puy-de-
D&me), the Drachenfels, and Hungary. Many opals, treated with
solution of potash, leave crystals, as those from Zimapsn, Easchan,
Silesia, and the cacholong from Iceland. Where such crystals
are abundant, tho opal becomes opaque or snow-white. Jeozsch
regards these as still another variety of silica.
890
MINERALOGY
187. Opal, »SiO„ HjO to SSiOj, HjO .
Amorphous; "fracture conchoidal ; very brittle. "H. "5"5 to
3*6; G. — 2 to 2'2. Tiansparent to opaque; vitreous, inclining to
rtisinous. Colourless, but often white, yellow, red, brown, green,
or grey, with a beaufeful play of colours. B. B. decrepitates and
becomes opaque, but is infusible; in the closed tube yields water;
almost wholly soluble in solution of potash. Co. : silica, with 5 to
13 per cent, water. Most opals are mixtures of various minerals.
The following varieties may be noticed: — (1) Syalile, Glassy Opal,
or MUlUr's Glass: transparent, colourless, very glassy; small botry-
oidal, or incrusting; Kaiserstuhl in the Breisgan, Schemnitz, Silesia,
Moravia, Mexico, and other places. (2) Fire Opal or Girasol: trans-
parent ; brilliant vitreous lustre ; bright hyacinth-red or yellow ;
Zimapan in Mexico, and the Faroes. (3) Noble Opal, semi-trans-
parent or translucent; resinous, inclining to vitreous; bluish or
yellowish white, with brilliant prismatic colours; most show double
refraction and are binaial; in irregular masses or veins near Eperies
in Hungary;Au3tralia, (4) Common OpaU semitransparent, vitreous;
white, yellow, green, red, or brown; Hungary, also Faroes, Iceland,
the Giant's Causeway, and the Western Isles of Scotland. (5)
Semi-opal: duller and less pellucid; Wood Opal or Lithoxylon: with
the form and texture of wood distinctly seen; Hungary, Bohemia,
and other countries. (6) Menilite: compact, reniform; opaque and
brown or bluish grey; Menilmontant, near Paris, (7) Opal Jasper:
blood-red, brown, or yellow. (8) Cacholong: opaque, duU, glimmer-
ing, or pearly, and yellowish or rarely reddish white; in veins or
reniform and incrusting ; Faroes, Iceland, the Giant's Causeway. One
variety is named Bydropkane, from imbibing
■water, and becoming translucent. (9) Siliceous
SiTiter: deposited from the Geyser and other
hot springs; and Feari Sinter: incrusting
volcanic tufa at Santa Fiora in Tuscany
{Fiorite), and in Auvergne.
138. Zir.coN, ZrOa, SiOj .
Pyramidal ; P 84° 20'. Crystals, ooP, P ;
often with 3P3 ; also ooPoo, P; or ooPoo {s),
ooP (0, P (P), 8P3 {x), P« {t), 4P4 (3/), 6P5 {z),
(fig. 318, also 86, 87, 585). Chiefly prismatic
or pyramidal, and in rounded grains. Trans-
parent to opaque ;
vitreous, often ada-
mantine. Rarely
white, generally grey,
yellow, green, or fre- (^
quently red and ■^'
brown. B.B. loses
its colour, but is in>
fiisible. Not affected
by any acid except
concentrated s. -acid,
after long digestion.
C.c. : 66 '3 zirconia
and 337 silica, mth
0 to 2 iron peroxide Fig. 318. Fig. 319 (sp. 138).
as colouring matter. Miaslc, Arendal, Sweden, Belgium (at Nil-St-
Vincent), Carinthia, Tyrol, Ceylon, and North America; in Scot-
land, Scalpay in Harris (fig. 319), Lewis (Byacinth), Sutherland,
Ross. The colourless varieties are sold for diamonds. The more
brilliantly coloured are named hyacinths, and are valuable gems.
SULPHIDES, SELENIDES, TELLURIDES, &c.
139. Ptrite, FeSa .
Cubic ; scmitesseral dominant (figs. 320 to 323, also 67 to 77, and
26 to 34). Pentagonal-dodecahedron in excess; or strife, produced
by oscillation of it with faces of the cube, visible. Often distorted,
as in the cubo-octahednil twin (fig, 323). Sometimes massive and in
pseudomorphs. CI. cubic or octahedral, difficult; brittle. H. -6
Fig. 320.
Fig. 821.
Fig. 322.
to 6*5; G. — 4*9 to 5 '2. Brass-yellow, often somewhat gold*
Yellow; streak brownish black, when broken omits smell of
filphur. In closed tube suJnliur suhlimea. B.B. on charcoal
burns with blue flame, and ouour of Bulphiirous acid. In inner
flame fuses to magnetic bead. Sol. in n. acid, with deposition of
sulphur. Co.: iron 46*7, sulphur C3'3; often contains gold in visible
grains, when broken, Common to rocks of all ages. Tomnadashin,
Fig. 324.
Fig. 325.
Fig. 326.
Bimam, Scotland; Cornwall, Englan,;; Eib.iand Traversella; Peni;
Rossie, Middletown, and Schoharie in U.S. ^urlUi-'-vs pyrites,
Berezoff (Siberia), Adelfors (Sweden), Mexico. Used to be cut in
facets and set as an ornament,
under the name of marca-
sitcs; also for striking fire in
the old firelocks, whence tha
name of firestone; now used
for manufacture of sulphuric
acid.
140. Makcasite, FeSj.
Right prismatic; ccp(i/)
106" 6'. Crystals tubular, thin
prismatic, or pyramidal. ^'S- 323 (sp. 139).
Twins very frequent, also cockscomb-like groups, or spherical
and stalactitic. CI cop; fracture uneven; brittle. G.-4-65
to 4 "9. Greyish bronze-
yellow to greenish grey,
often with brown crust ;
streak greenish grey or
brownish black, B.B., &c.,
like pyrite. Very prone to
decomposition, being changed
into green vitriol, which may
be detected by the tongue.
Spear Pyrites are twins like
fig. 325 ; Littmitz, Przibram. Bepatic Pyrites or Lelcrhics, liver-
brown, generally decomposing; Harz, Saxony, Sweden. Codcscomh
Pyrites; Derbyshire and the Harz. Kyrosite contains arsenic.
141. MispiCKEL, FeSo + FeAs.
Right prismatic ; ooP {M) 111" 12' (fig. 326).
massive or columnar. CI. ooP; fracture
uneven; brittle. H. = 5"5 to 6; G. «6
to 6*2. Silver- white to steel-gr*;y ;
streak black. In closed tube yields
first a red then a brown Bublimate,
lastly metallic arsenic. B.B. on char-
coal fuses to a black magnetic globule.
Sol. in n. acid, with separation of
arseaious acid and sulphur. Co.: 34'3
iron, 46'1 arsenic, 19*6 sulphur; some-
times silver or gold, or 5 to 9 of cobalt
Cornwall, Freiberg, Ziunwald, Sweden, Franconia, America.
142. Leucoptrite, FeAs.
Right prismatic ; ooP {d) 122° 26'; Poo (o) 51^20'.
fig. 327; generally massive or columnar. CL basal;
fracture uneven; brittle. H. = 5 to 5'5 ; G. =-7 to
7 '4. Silver-white with darker tarnish; streak greyish
black, B. B. emits strong smell of arsenic, and fuses
to a black magnetic globule. C.c, i iron 272,
arsenic 72*8 , sometimes iron 32'2 and arsenic 66 S ;
always some sulphur, and often nickel and cobalt.
Fossum in Norway, Andreasberg, Stj'ria, and Silesia.
Spathiopyrite, from Bicber in Hesse, seems a variety.
143. CoBALTiTE, CoSa-l-CoAs.
Cubic and hemihedral ; sometimes massive (figs. 67, 74). CI.
cubic, perfect ; brittle. H. = 5-5 ; G. -6 to 6 '3. Brilliant lustre.
Pinkish silver-white ; tarnishes yellow or grey ; streak greyish
black. B.B. with borax blue glass; evolves smell of arsenic. C.c:
cobalt 35"9, arsenic 44'9, sulphur 19*2. St Just in Cornwall,
Tunaberg in Sweden, Skutterud in Norway, Querbach in Silesia.
144. Glaucodote, (Co, Fe)Sa + (Co, Fe)A8j,
Right prismatic; ooP 112° 36'. CI. basal, perfect H.-£;G.-
6. Lustre metallic. Greyish white ; streak black. C.c. : cobalt
247, iron 11*9, arsenic 43*2, sulphur 20*2. Huasco in ChilL
145. Smaltine, (Co, Fe, Ki)As3.
Cubic ; generally like fig. 27 ; also reticulated and granular com-
pact. CI. octahednil ; fracture uneven; brittle. H. -5'5; G. —
6*4 to 7 '3. Tin-white to stccl-grey, with darker iridescent tarnish ;
streak greyish black. Evolves odour of arsenic, when broken or
heated. C.c: 71 "4 arsenic, 28'6 cobalt; sometimes 3 to 19 iron,
and 1 to 12 nickel, or 4 bismuth. Dolcoath ond Redruth in
Cornwall, Scbneeberg, Annaberg, Tunal>erg, Aileuiont, Chatham
in Connecticut.
146. CuLOANTiTK(fr/ii:te JV^icJte/), NiAs.
Cubic ; generally fine granular or compact ; fractnr« uneven ;
brittle. H.-6-6; G. "64 to 6 6, Tin-white, rapidly tarnishing
black. In the closed tubo yields a sublimate of arsenic, and
becomes copper-red. Gives odour of arsenic when brokeu. B.B.
fuses with much smoko, becomes coated with crystals of arscuious
acid, nnd leaves a brittle grain of metal. C.c: 28-2 nickel, 71 «
arsenic, but often with cobalt Schnoebei^, Riechclsdorf, AUe-
mont, Chath:;m in Connecticut
Crystals like
Fig. 327.
MINERALOGY
391
Ail, 0Bm>0BiTnx, NiSi + KiAs,.
_,/Oabic (figa. 74, 30, 26). CL cubic, generally grannlar. H. - 6 -J ;
0.-6 '67. Lostio meUllic. Silver- white to steel-grcy, decrepitates
in closed tnbe. B. B. fuses to a blaclc slag ; partially soL in n. acid.
O.c; S5'2 nickel, 45*4 arsenic, and 19'4 sulphur; sometimes
with cobalt. Craignair, n«ar Loch F^e, with 23 nickel and 6
cobalt. The Harz, Sweden, Spain, and Brazil.
148.. TJllmankite, NiSb+NiS,.
Cubic (fi^ 31, 29, 27) ; often tetrabedial, and in twins as in
Bgs. 323, 329. CL cubic, perfect; fracture nneveiL H. -5 to S'S ;
ti. -8 2 to 6 '6. Lead-grey to tin-white, often with iridescent
Fig. 328.
Fig. 329.
tarnish. B.B. fuses with dense fumes. SoL inn. acid. C.c. : 27°4
ftickel, 57*5 antimony, and 15*1 sulphur. Westerwald, Siegen,
Harzgerode, Lolling (Carinthia), Lobenstein, and Bleiberg.
149. Raumelsbebqite, NiAs.
Right prismatic ; ooP 123° to 124°. Chiefly massive, or in radiating
and botryoidal aggregates. H. -6; 6. —7 '2. Colour tin- white.
Schneeberg, Reichelsdorf, and Wittichen in Baden.
150. Haueeite, MnSj.
Cubic (figs. 30, 30-26, 30-33-37). Crystals single or in spherical
f roups. CT. cubic, perfect ; H. = 4 ; G. = 3 ■46. Reddish brown to
rownish black ; streak brownish red. In closed tube yields sul-
phur, and leaves a green mass, which is sol. in h. acid. C.c: 46
manganese and 54 sulphur. Ealinka in Hungary.
151. PlTEEHOTiTE (Mognetin Pyrita), Fe7Sj.
Hexagonal; P 126° 48'. Crystals rare, sometimes hemihedral on zj,
commonly massive or granular. CL <»P, imperfect ; brittle. H. —
3 '6 to 4 '6 ; G. — 4 '5 to 4 "6. Colour bronze-yellow with pinchbeck-
brown tarmsh ; streak greyish black. More or less magnetic. C.c:
Fig. 330.
Fig. 331.
«S"65 iron and 36 35 sulphur ; sometimes with nickel. Common in
primary limestones and diorites of Scotland. Crystallized in above
forms at Aakaig, on Loch Shin, Sutherland ; Carnarvon, Cornwall,
Fahlun, Bodenmais, Andreasberg. Distinguished by its colour
and its solubility in h. acid.
152. Lnra.siTE, 2(Co, Cu)S + CoSj.
Cubic (fim. 29, 30) ; often twinned ; twin face 0 ; also massive.
CL cubic ; brittle. H.-5-5; G.-.4-9 to 5. Silver-white, with a
yellow tarnish ; streak blackish grey. B. B. fuses to a grey mag-
netic globule, which is bronze-yellow when broken. C.c: cobalt
432, copper 14-4, iron 3-5, sulphur 33-5. Bastnacs (Sweden).
153. SlEOESiTE, CoS-(-Ni5S,(!).
Cubic ; generally in crystals like fig. 29 ; also massive. Colour
silver-white, inclining to pink. Other features like linnaite. C.c:
cobalt 40-8, nickel 146, sulphur 431. Miisen near Siegen, Mary-
land, and Missouri. The American mineral has 30 '5 of nickeL
164. POLTDTMITE, Ni,S,.
Cubic ; in minute octahedral crystals and flattened twins. CL
mbic. H. -4-5; G.-4-81. C.c: 39-45 nickeL 4055 sulphur, but
generally with 4 of iron. Westphalia. Saynitt or grunauUe seems
to be a bismuthic and cobaltlo raristy ; it ia from Gronan in Sara-
>Utenkirchen.
Tig. 332.
Leadhills, Peritland Hills,
155. Bthiohkite, 3Ni3 + 2NiS,.
H. -3 to 3-5; G.-47. C.c: 64-23 nickel, 2-79 Iron. 42-8«
sulphur. From the Westerwald.
156. HoBBACHiTE, 4FeJS,•^Ni3S,.
Crystalline masses. H. -4 -5 ; G. -4-43 to 4-7. Colour pinch-
beck-brown ; streak black. C.c. : nickel 11 98, iron 41 '96, sulphur
46-87. Horbach in the Black Forest.
157. SKUTTEEUDiTB, CoAs, .
Cubic (figs. 30, 26 with ZZ, 40) and granular. CL cubic ; frac-
ture conchoidai ; brittle. H. =.6 ; G. -6 74 to 6 84. Tin-white to
lead-erey. Lustre brilliant. In closed tube gives sublimate of
metallic arsenic, otherwise like smaltine. C.c: 79 arsenic, 21
cobalt Skutterud, near Modnm in Norway.
168. Galena, PbS.
Cubic ; crystals chiefly cube, octahedron, and rhombic dodeca-
hedron ; rarely 20 and 202. Also massive and granular, compact,
or laminar, and in pseudomorphs of pyromorphito and othw
minerals. CL cubic, very perfect;
fracture scarcely observable ; sectile.
H. = 2-5; G.-7-2 to 76. Lead-
grey, with darker or rarely iridescent
tarnish ; streak greyish black. B.B.
decrepitates, fuses, and leaves a
globule of lead. SoL in n. acid.
Co.: 86-7 lead, and 13 3 sulphur;
but usually contains a little silver,
ranging from 1 to 3 or 6 parts in
10,000 ; rarely 1 per cent, or more.
Some contain copper, zinc, or anti-
mony, others selenium, and others
(the "supersulphuret") probably free
sulphur (2 to 8 per cent.). Most
common ore of lead in many countries.
Linlithgow, Inverkeithing, Monaltrie, Tyndrum, Strontian, Islay,
Orkney, Cornwall, Derbyshire (Castletown), Cumbcrhtnd (Alston
Moor), Durham (AUenhead), Wales, Isle of Man.
159. CtTPBOPLUMBITE, 2PbS -H Cu^S .
Cubic H. =.2-6; G. =6-4. Bluish grey. Chili.
160. Beeoebite, ePbS-l-BijSj.
Cubic. G. = 7-27. CL cubic. Light to dark grey. Lustre bi-illiant.
C.c: sulphur 15, bismuth 20-6, lead 64-2, with copper 1-7. Grant
(Park county, Colorado).
161.- Clatjsthalite, PbSe.
Cubic; but massive granular. H. — 2 5 to 3; 0. = S'2 to 8-8.
Lead-grey; streak grey. B.B. fuses, smells of selenium, colours
the flame blue, stains the support red, yellow, and white, and
volatilizes, except a small residue, without fusing. C.c. : 72-7 lead,
27-3 selenium ; but sometimes 11-7 of silver, Zorge, Lerbach, and
Clausthal in the Harz. Tilkerodite, or Sden^Cobalt-Blei, containing
3 per cent, of cobalt, fr jm Tilkerode, is a vaiiety.
162. ZOKGITE.
Massive granular ; like clausthalite, but inclining to reddish, and
often tarnished. There are four varieties, (a) Selen-Blei-Kuf/cr :
G. — 7 -4 to 7 -5 ; 5PbSe -I- CuSe ; with 4 copper, 65 lead, 30 selenium.
(6) The same, butwith G. -5-6 ; 4Pb, 4Cu, 7Se ; with 158 copper,
48-4 lead, and 35 selenium, (c) Sden-Eup/er-BUi: with G. -7;
2PbSe -I- CuSe; with 8 copper, 57 lead, and 32 selenium, (d) 2PbSa +■
9CuSe ; with 46-64 copper, 16-58 lead, and 36-59 selenium. From
Tilkerode and Zorge in the Harz, and near Gabcl in Thuringia.
163. Altaite, PbTe.
Cubic and granular; fracture uneven ; sectile. H.— 3 to 3-6; G.—
8-lto8-2. Tin-white to yellow, with yellow tarnish. B. B. coloura
the flame blue, fusing to a globule, which almost wholly volatilizea
C.c. : 61-9 lead and 38-1 tellurium. ZavcdinsH in the Altai,
California, Colorado, and ChilL
164. REDEn-rHTTE {Copper Glance), CujS.
Right prismatic ooP (o) 119° 35'; P (P) middle edge 125° 22';
if (o) middle edge 65° 40'; 2P<o {d) middle edge 125° 40'; J?oo («)
middle edge 65° 48'. Crystals OP («), ooP (o), cb?oo (p) (figs. 838
Fig. 333. Fig. 334.
834); with hexagonal aspect; also twins; and massive. CL ooP,
imperfect ; fracture conchoidai or uneven ; sectile. H. — 2 6 to $ j
392
MINERALOGY
G. -60 to 6-8. Eathcr dull; brighter on tho streak. Blackish
lead-grey, with a blue or other tarnish. B.B. colours tho flame
blue ; on charcoal in the oxygen flame sputters, and fuses easily ; in
the red. flame "becomes solid. With soda gives a grain of copper.
Green solution in n. acid, leaving sulphur. Cc: 79-8 copper, 20-2
sulphur. Fassnet Burn (HaddiDgtonshire), Ayrshire, Fair island,
near Kedmth and Land's End in Cornwall, Saxony, Silesia, Nor-
way, tho Banat, Siberia, and the United States. Important copper
ore.
165. Stkometerite, CujS + AgS.
Right prismatic ; isomorphous with redruthite. Crystals rare ;
osually massive ; fracture flat, very sectile. H. -2-5; G. -6-2 to
ii-3. Bright. Blackish lead-grey. Cc. : 53-1 sUvcr, 31-2 copper,
and 157 sulphnr, but often indeberminat* proportions of silver (3 to
63) and copper (30 to 76). SchUngenbeac in Siberia, Rudelstadt in
Silesia, and Catemo in Cliili.
168. Berzelinite, CujSe.
Crystalline, in thin dendritic crusts, and imbedded in calcite.
Silver-white with a black tarnish ; streak shining. In open tube
gives a red sublimate of selenium, with white crystals of selenious
acid. B. B. on charcoal fuses to a grey, slightly malleable bead,
giving odour of selenious acid; with soda a grain of copper. Cc. ;
61 '5 copper and 33 '5 selenium. Skrikerum in Smiland, Lerbach
in the Harz.
167. CuooKESiTE, (Cu'n)jSo.
In crystalline grains the size of peaa, H. -2-6 to 3; G. -6-9.i
Brittle. Lead-grey. Metallic. B.B. colours the flame intens^'^
green. Cc: 4576 copper, 371 silver, 17'25 thallium, 35''27
selenium. From Ski-ikcrum.
16S. EcKAiRiTE, CuoSe-f AgSo.
Massive and granular crystalline. Cuts with knife. Lead-grey ;
streak .shining. B. B. fuses to a brittle metallic grain. Cc. :43'1
silver, 25 3 copper, and 31 '6 selenium. Skrikerum, Atacama, Chili.
169. Argentite, AgjS .
Cubic. ooO=o ; O; ooO; and 202 (figs. 29, 56). Crystals generally
misshapen, with uneven or curved faces ; in druses, or linear
groups ; olso arborescent, capillary, or in crusts. CI. indistinct ;
fracturu hackly ; malleable and flexible. H. =2 to 2*5; G. = 7 to
7*4. K.irely brilliant, more so on tho sti-eak. Blackish lead-grey,
often with a black, brown, or rarely iridescent tarnish. B.B. on
charcoal fuses, intumesces greatly, and leaves a grain of silver.
SoL in con. n. acid. Cc. : 87 silver and 13 sulphur. Huel
Duchy, Dolcoath, Herland, and near Callington in Cornwall ;
Alva in Stirlingshire: Freiberg, Marienberg, Annaberg, Schneeberg,
Johann-Georgenstadt, JoachimsthaJ, Schemnitz and Kremnitz,
Kongsberg. Common ore at Guanajuato and Zacatecas in Mexico,
in Peru, and at Blagodat in Siberia.
170. ACANTHITE, AgS .
Right prismatic. H. =2-5; G. =7-33. Iron-black. Cc. Kke
argentite, thus dimorphcus. Freiberg and Clausthal, on argentite;
also at Copiapo.
171. Jalpaite, 3AgS-fCn3S.
Cubic; form 0. CI. cubic; malleable. H. -2-6; G. -6-88. Dark-
grey. Metallic lustre. Cc: silver 7178, copper 14'04, aulphar
li'2. Jalpa in Mexico.
172. Lautite (CiLAg) As.S.
Granular. Iron-black. H. -3; G. -4-96. Cc: copper 28 '3,
silver 12, arsenic 41-8, sulphur 17 '86. Lauta, near Marienberg.
173. Nadmannite, AgSe.
In thiu plates and granular. CI. hcxabedral, perfect. Malleable.
H. -2-6;G. -8. Iron-blaok. Splendent. Co.: 73 silver and 27
selenium, with 4-91 lead. Tilkerodo.
174. Hessite, AgTe.
Cubic or anorthic(?) ; massive and granular. Slightly malleable.
11.-2 5 to 3; G. -8-1 to 8-4.5. Blackish lead-grey to steel
grey. B.B. on charcoal fumes, fuses
spots, and leaves a brittle grain of
silver. Cc: 62-8 silver and 37-2
tellurium. Zavodinski (Altai), Nag-
yog, Rctbunya, California, and Chili.
175. Petzite, 2AgTe-f AuTe.
Like hessite. Two varieties : —
(o) with G. -8 72, containing 18 per q
cent of gold, from Nagyag ; (6) with
G. -9 to 9-4, and 24 to 26 of gold.
Calaveras and Tuolumne in Cali-
fornia, Colorado.
176. DisoBASITE. AgnSb ; AgjSb ;
and AgjSb.
Right prismatic; P with polar
cdgpa 132" 42' and 92°; ooP 120°
aeaily (figs. 335, 336). Crysluls ahort iitlamalic, or thick tiibul
and vertically striated (fi^. 335) ; twins nnited by a foes of xP ;
often in stellar groups (hg. 336) ; also massive or gronalw. (3.
basal and Pco, distinct; o>P imperfect ; rathe
brittle, and slightly malleable. H. -3-5
G. -9-4 to 9-8. Silver-white to tin-white, witli
a yellow or blackish tornish. B.B. fuses easily,
fumes staining the charcoal white, and leaves
a gMin of silver. Sol. in n. acid. Cc. : 64
to 84 silver, and 36 to 16 antimony. Andreas-
berg, Allemont in Dauphine, Spain, and Ar-
^neras in Coquimbo (Chili),
tains
Fig. 336.
valuable ore of silver. A variety
1 silver and 5'8 antimony, and is Ag,eSb.
Fig. 837.
to a black grain with white
from Chili
177. Blende, ZnS.
Cubic and tetrahedral (figs. 152, 153, 337). Twins remarkably
common, united by a face of 0, and several times repeated ; fre-
quently massive and granular. CI. o=0, perfect ; very brittle. H. -
3"5to4; G. ■= 3 '9 to 4 "2. Semitransparent to opaque ; adamantine
and resinous. Brown or black, also
red, yellow, and green, rarely colour-
less or white. B.B. decrepitates, often
violeutly, but only fuses on very thin
edges. Sol. in con. n. acid, leaving
sulphur. Cc: 67 zinc and 33 sulphur;
but generally in the darker varieties
with 1 to 15 iron, 0 to 3 cadmium.
Very abundant. Glen Gaim (bright
yellow and highly phosphorescent),
Leadhills. Tyndrum, (Cornwall, Derby-
shire, Cumberland, the Harz, Freiberg,
Przibram, Schemnitz, Kapnik, North
America, Peru. Used for producing zinc vitriol and sulphur, and
as an ore of zinc. Lithium, indium, thallium, and galliam bar*
all been found in blende.
178. Witrtzite, 6ZnS-(-FeS.
Hexagonal ; ot.P, P, with well-marked horizontal striee. CI.
basal, and prismatic. H. = 3"5 to- 4 : G. — 3*9 to 4'1. Brownish
black ; streak light brown. Cc. : like blende, which is thus dimor-
phous. Oruro in Bolivia, and Przibram (radiated and cadmiferous).
179. Greenockite, CdS .
Hexagonal, and generally hemimoqihic PS6''21'; 2P 123° 64'.
Crystals 2P, OP, 00 P, P; orP, 2P, ooP; attached singly. CI. »?,
imperfect; basal perfect. H. -3 to 3-5; G. -4-S to 4 9. Trans-
lucent; brilliant resinous, or adaman-
tine. Honey- or orange-yellow,
rarely brown ; streak yellow. B.B.
decrepitates, and becomes carmine-
red, but again yellow when cold ;
fused with soda forms a reddish
brown coating on charcoal. Sol. in
h. acid. -
Fig. 338.
C.cT: 776 cadmium, and 224 sulphur. Bishopton ia
Fig. 335 («p. 176).
Renfrewshire; Przibram, and Friedensville in Pennsylvania.
180. Alabandine, MuS.
Cubic ; O and ccOoo ; usually massive and granular. CI. hexs-
bedral, perfect; fracture uneven; rather brittle. H. — 3"5 to 4;
G. ■=3'9 to 4. Opaque ; semi-metallic. Ii-on-black to dark steel-
grey, brownish black tumish ; streak dark green. B.B. fuses on thin
edges to a brown slag. Sol. in h. acid. C.c. : 63 manganese and
37 sulphur. Nagyag, Kapnik, Alabanda in Caria, Mexico, and
Brazil.
181. MiLLERITE, NiS .
Hexagonal rhombohedral ; R 144° 8'; in fine acicular prisms
of aP2, R. Brittle. H.-3-5: G.-4-6(or6-26to6-65). Ijrass-
or bronze-yellow, with a grey or iridescent tarnish. B.B. fuses
easily to a blackish metallic globule, which boils and sputters.
In nitro-hydrochloric acid forms a green solution. C.c: 64 '4 nickel
and 35 -6 sulphur. Morven (Argyllshire), Chn]>el (Fife), Ayrshire,
near St Austell in Cornwall, at McrthjT-Tj-dvil, Johann-Georgen-
stadt, Joachimsthal, Przibram, Camsdorf, Kiccbelsdorf, Pennsyl-
vania.
182. Pentlanbite (£«<n>itci«?Kfe), 2FeS-fNiS.
Cubic ; massive ond granular ; fracture uneven ; brittle. H. —
3'5 to 4 ; G. — 46. Light pinchbeck-brown, with darker streak.
Not niagni'tic B.B. acts in general like pyrrhotito ; the roosted
powder fonns with boiax in the red. flame a blnck onaquc glass.
C.c: 36 sulphur, 42 iron, and 22 nickel ; but mixed witJ»pyrrhotit€
and cbalcopyrite. Lillehamuier in southern Norway. InKrarils,
5FeS -H NiS, with 11 of nickel, from near Inveraray, is a variety.
183. NlCKELiTE (C(7>fKr A'icM), NiAs.
Hexagonal ; P 86° 50'. Crystals <»P, OP ; rare. Arborescent,
ri niform, and massive ; fracture coachoidal ond uneven ; britilo.
11. -5 5 ; G. -76 to 7 7. Ligl icrpperied, with a blockish tarnish.
It forms no sublimate in tb.e closed tube. B.B. fuses with stifcug
MINERALO(:J¥
^93
AUne^to s white, brittle, loetallic globule. C.c: 48 '6 nickel and
564 arsenic Hilderston in Linlithgow, Pibble in Kirkcadbright,
LeadhilU, Pengelly and Huel Chance in Cornwall, Freiberg, Schnee-
berg, Joachimsthal, Saugerhausen, Andreasberg, Chathani in Con-
jiectieat. Used as an ore of nickel.
^S4. BailTHAjrPTiTE {Jntirrumial Nicitt), NiSb.
Hexagonal ; P 86° 66'. Crystals, thin striated hexagonal tables
Bf OP, »P. H. - 5 ; G. - 7 -5 to 7 6. Brilliant Light copper-red,
generally with violet tarnish. B.B. fames, bat foses with great
rifficalty. C.c: 32-2 nickel and 67-8 antimony. Andreasberg.
185. SriOTJiTK {Tin Pj/riUa), 2Ca9, SnSj + 2(FeS, ZnS) + SnSj.
Onbic ; in cabea very rare, generally massive and granular. CL
liexaltedral, imperfect ; fracture nneven , or small conchoidal ;
brittle. H. -4; G. -4-3 to 4-5. Steel-grey ; streak black. C.c:
26 to 32 tin, 24 to 30 copper, 6 to 12 iron, 2 to 10 zinc, and 30
salphor. Huel Rock near St Agnes, St Michael's Mount, and Cam-
"broa in Cornwall; Zinnwald. Bell-metal ore.
186. Steknberoite, (AgS -h 2FeS)FeS, .
Right prismatic; P middle. edge 118°. Crystals usually thin
tabular; in twins, or in fan-like and spheroidal groups. CI. basal,
lurfect ; sectile, and flexible in thin
laminae. a = l to IS; G.-4-2 to
4*25. Dark pinchbeck-brown, often
a violet-blue tarnish ; streak black.
O.C.: 34-2 silver, 86-4 iron, and 304
sulphur. Joachimsthal, Schneeberg,
«nd Johann-GeorgensUdt. Flexible '^Z- ^■^^■
SulphuTct of Silver, from Hungary and Freiberg, is identical. Frie-
ttiU, AgjFcjSj, in twins (fig. 339), is a variety.
187. RiTTIHOEEITE, AgAs .
Oblique prismatic. coP 126° 18' ; ooPoo and OP. CI. basal ;
fracture conchoidal; brittle. H.— 2 '5 to 3; G. = 5 63. C.c: silver
677, the remainder being arsenic, with someselenium. Joachimsthal,
Silesia, Felsobanya in Hungary.
188. COTELLINE, CuS.
Hexagonal. Crystals ooP, OP; rare; usually reniform and granu-
lar. CI. basal; sectile. Thin laminffi flexible. H. -16 to 2 ; G. -
3 •a to 46. Resinous. Indigo-blue; streak black. B.B. burns
■with blue flame. Sol. in n. acid. C.c: 667 copper, 33'3 sulphur.
Caimbeg in Cornwall, Vesuvius, Leogang (Austria), Chili, Angola,
New Zealand, and Victoria. ~
189. Chalcoptbite (Ciyper i»jn-i<M), CuS■^FeS.
Pynmidal ; and sphenoidal hemihedric ; JP (P) with polar ed^es
71° 20' ; oaPoo. Crystals generally small and deformed; twins
very common, like fig. 840. Poo (6) 69° 10', 2Pco(<:) 126° 11',
<)P'(n), P (fig. 89). Uost commonly compact and disseminated;
also botryoidal and reniform. CL pyramidal 2Po:> ; some-
times rather distinct; fracture conchoidal or nneven. H. — 3'5to
4; G. — 4-1 to 4 '3. Brass-yellow, often with a gold-yellow or
iridescent tarnish (peacock copper ore) ;
streak greenish black. B.B. on charcoal be-
comes darker or black, and on cooling red;
fuses easily to a steel-grey globule, which at
length becomes magnetic, brittle, and greyish
red on the fractured surface ; with borax and
aoda yields a grain of copper; moistened with
b. acid, colours the flame blue. C.c. essenti-
ally 1 atom copper, 1 atom iron, and 2 atoms
sulphur; with 345 copper, 30-6 iron, and 35 "S- S*'-
sulphur. The most abundant ore of copper. In Kirkcudbright-
shire and "Wigtownshire, Tyqdrum in Perthshire, Invemess-shire,
Lairg in Sutherland, Shetland, Anglesea (Park's mine), Derbyshire,
Staffordshire, Cumberland, Ounnislake (Devonshire), St Austell
(Coi'nwall), Wicklow, Falun, Rbraas, Freiberg, Mansfeld, Goslar,
Lauterberg, Miisen, Siberia, ft is distinguished from pyrite by
yielding readily to the knife, by its tarnish, and by forming a green
solution in n. acid.
190. BOENITE {Purple Copper), SCu^, Fe^S^ .
Cubic. Crystals ooQoo, and ooOoo, O; but rare, and generally
rough or uneven ; also twins. Mostly massive. CI. octahedral ;
fracture conchoidal ; slightly brittle ; sectile. H. =• 3 ; G. = 4 9 to
5 1. Colouf between copper-red and pinchbeck-brown, with tarnish
at first rod or brown, then violet or sky-blue ; streak greyish black.
B. B. acts like chalcopyrite. Soluble in con. h. acid, leaving sulphur.
C.c: 66-6 copper, 16-4 iron, and 23 sulphur. Crystals near Rcdnith
and St Day in Cornwall ; massive at Killarney in IreLand ; also
N«rway, Sweden, Mansfeld, Silesia, Tuscaay, and ChilL An ore of
copper,
191. iCoBAN, CuS, FcjSj'
Cubic H. -"i; G. -"4"1. Bronze-yellow; streak bronze-yellow and
tilack. Barracanao in Cuba, Tunaberg and Esfveltorp in Sweden.
11)2. DOHEYKITE, Cu„A9 .
Botryoidal or massive ; fracture uneven ; brittle, n. — e to S-6 ;
G. — 7 to 7 "6. Tin- or silver-white, inclining to yellow, with an
iridescent tarnish. Not affected by h. acid. C.c: 71 "63 copper and
28 '37 arsenic Calabnzo in Coquimbo, and Copiapo in Chili. C(m-
dwrri^ massive, seems an impure variety ; from Condurrow mine and
near Redruth (Cornwall). AlgodoniU from Lake Superior, W^i^
neyite from Mexico, and Darvnnite (88 copper) arev aUo identical
or similar.
193. Melonite, NijTcj.
Hexagonal ; minute tabular crystals, foliated and granular.
Metallic lustre. Reddish white; streak dark grey. C.c. : nickel 21,
silver 4'1, tellurium 73°4; Stanislaus and Calaveras (California).
1?4. Syitakite, AgTcj-HAuTe,.
Oblique prismatic, C 65° 21'. a.P 94° 26'; - P»to 19° 21'; P"oo
62° 43'. Crystals small, short acicular, and often twinned and grouped
in rows like letters ; sectile, but friable. H. — 1 '5 to 2 ; G. — 7 '99 t«
Fig. 341. Fig. 342.
8 "33. Steel-grey to silver-white, and pale bronze-yellow. C.c. : 59 "o
tellurium, with 0 6 to 8 '5 antimonv, 26 '5 gold (in some 30), and
13"9 silver, with 0'2 to 15 lead. Oftenbanya {Graphic Tellvri-um),
Nagyag ( Tellow Tellurium), and California.
195. Naoyaqite, Slack Tellurium.
Pyramidal. P 137° 52'; Pco 122° 60'; and OP (fig. S43). Crystals
tabular, rare; in general in thin plates or foli-
ated. Ch basal, perfect; sectile ; thin lamin%
flexible. H.-l to 15; G. -685 to 72.
Splendent. Blackish lead-grey. C.c: 51 to
63 lead, 6 to 9 gold, 1 copper and silver, 13 to
32 tellurium, 3 to 12 sulphur, and 0 to 4 5
antimony, Nagyag and Offenbanya in Tran-
sylvania.
196. Maldonite, AUjBi.
H.-1-6 to 2; G.=8-2 to 97. Colour
silver-white, with black tamisfi. C. c. : gold ^- 3^3 (sp. 195).
64 °6, bismuth 35 '6. Occurs in granite veins at Ualdon in Victoria.
197. Chile.xite, AgjjBi.
Minute plates of metallic lustre. Silver-white, but tarnisuea red
or yellow. Silver 83 9, bismuth 16 1. From the mine Sas
Antonio near Copiapo in Chili.
198. CiNNABAE, HgS.
Hexagonal and rhombohedral; R71°4S'. R(n),0R(o),ooE (nn, {R
(i) (fig. 344). Ciystals rhombohedral; also
gi-anu^r, compact, and earthy. CI. ooB,
perfect ; fracture uneven and splintery ;
sectile. H.-2 to 25; G.=8to8-2. Traus-
parent, with circular polarization. Adaman-
tine. Cochineal-red ; streak scarlet. C.c:
86 2 mercury, 13-8 sulphur. Idria in Camiola,
Almaden iu Spain, Wolfstein in Bavaria,
Saxony, Hungary, Tuscany, China, Call- '"'?■ ***•
fornia, Mexico, Peru. Chief ore of mercury. Also a pigment.
Bepaiic Cinnabar is a bituminous mixture.
199. TiEMANNITE, HgSe.
Finegranular; brittle. H. =2'6; G. =7'1 to 74. Brilliant. Dark
lead-grey. C.c. : 75 mercury, 26 selenium. Clausthal and Zorge.
200. Lekbachite, (PbHg)Se .
Granular and massive G, -7'8 to 7 88. Colour stc8l-gr«y to
iron-black. Brittle. Lerbach, Tilkerode in the Harz.
201. Ghanajtatite, Bi^Se,.
Massive; granubr; foliated and fibrous. n. = 2-5 toS;G.=e-25.
Blue-grey; streak grey and shining. Metallic; soft and malleable.
C.c: selenium 34-3, sulphur 7, bismuth 65. Santa Rosa (Qnanft-
juato, Mexico).
XVI. — SO
394
MINERALOGY
Fig. 346 (ap. 206).
202. COLORADOITE, HgTc .
Massive and gr.nnu'ar. H. - ^J; G. -8'63. MctalUo. Iron-black.
ConchoiUal fracture. Co.: 01 mercury, ?9 teUuiium. Colorado.
203. MOLTBDENITE, MoS .
Hexagonal (!). Crystals OP, kP; and OP, »P,P. Generally scaly.
CI. basal, perfect; sectile and flexible. Feels greasy. H. — ltol'6;
O. — 4'6 to 4 '9. Lead-grey with red tinge ; grey streak on paper,
greenish on porcelain. B.B. colours flame siskin-green ; on
charcoal yields sulphurous fumes,
and forms a white coating ; in warm
nitrochloric acid a greenish, and in
boiling 8. acid a blue solution,
C.c. : 69 molybdenum, 41 sulphur.
!n granular limestones, ana in '"' ^^''■
granites in Suthailand, Ross, Aberdeen, Argyll, and Kirkcudbright;
Shap in Westmoreland, Caldbeckfell in Cumberland, Arendal,
Zinnwald, Mont Blanc, Maine, Connecticut, Yea in Victoria. Used
for preparing blue carmine, for colouring porcelain.
204. IiAtraiTE, {RuOs)jSj.
Cubic. Crystals 0, ooOoo ; oo03, ooOoo. CI. octahedral H. =
7-5;G.-6-99. Metallic, bright Dark iron-black. Powdergrey.
Brittle. C.c. : ruthenium 66-18, osmium 3-03, sulphur 3179.
From platinum grains, in Borneo and Oregon.
205. Kealgar, AsS.
Oblique prismatic. ooPW74'26'; P«co(n)132° 2", coP°2 (0113°
16'. Crystals (fig. 346) generally prismatic;
sometimes massive. CL basal, also clino-
diagonal ; fracture splintery ; sectile.
H. -1-5 to 2; G. -3-4 to 3-6. Trans-
parent to opaque; resinous. Aurora-red ;
streak orange-yellow. C.c: arsenic 70,
sulphur 30. iTag
Gotthard, Vesuvius.
206. Oepiment, AsjSj.
Right prismatic. ooP 117" 49'. Fre-
quently foliated. CI. brachydiagonal ;
striated vertically ; sectile and flexible.
H.-1-5 to 2; G.-3-4 to 3-6. Semi-
transparent; resinous to pearly. Citron-
yellow and orange-yellow. Co.: arsenic 61, sulphur 39. Servia,
Kapnik, Andreasberg, Solfatara, Zi^lapan in Mexico.
207. DiMOErHiTE, AsjSs.
Eight prismatic. H.= 1-5; G. -3-58. Orange-yellow. Solfatara.
208. Stibnite, SbaSj.
Eight prismatic. P polar edges 109° 26' and 108° 21'; ooP 90° 64'.
Crystals (Sg. 347) generally prismatic. CL
brachydiagonal, perfect; sectile. H. —2;
G. -4-6 to 4-7. Brilliant lead-grey, often
tarnished. C.c: antimony 71 '8, sulphur
28 '2. Uaisley, Banffshire; Harehill,
Ayrshire ; Glendinning, Dumfriesshire ;
Endellion and Padstow, Cornwall ; Wolfs-
berg, Harz ; Przibram, Schemnitz,
Auvergae, Spain« America, Melbourne.
Chief ore "of antimony.
209. BlSMUTHINE, BL,33.
Eight prismatic ooP 91° 30'. Crystals
prismatic, striated ; also granular and
foliated. CL brachydiagonal ; sectile. p, „,y ,
H;-2to2-5; G.-6-4to6-6. Lead-grey. »- ' ^ ^'
C.c: 81'2 bismuth, 18'8 sulphur. Caldbeckfell (Cumberland),
Redruth (Cornwall), Riddarhyttan and Bastnaes (Sweden), Alten-
berg, Haddam (Connecticut), Ballarat (Victoria), Bolivia.
210. Fbenzelite, BijSej, or 2BijSe3-f Bi^Sj.
Eight prismatic ; ooP 90°. Needle crystals, and massive. CI.
brachydiagonaL H. -2-6 to 3; G. -6-25. Bluish grey; streak
greyish black, shining. Lustre metallic. Malleable. Co.: bismuth
€7-38. selenium 24'13, sulphur 66. Guanajuato (Mexico).
SULPHUR SALTS.
211. Guejakite, Cu2S-l-23bjS_,.
Right prismatic oo'p 101° 9'. CI. brachydiagonaL H
C. -5-03. Steel-green, with blui.ih
streak. C.c: copper 15'6, anti-
mony 58-5, sulphur 25. Gucjar in
Sierra Nevada.
212. MiAEOYaiTE, AgS-HSbSj.
Oblique prismatic, C 81° 36',
P 90° 63'; -P 69° 69'. Crystals
pyramidal, or tabular (fig 3-18);
massive ; sectile H. -2 to 2-6 ; F>g- S« (sp- 212).
G. -6'2 to 6'3. Metallic adamantine. Blackish lead-grey to steel
= 3-6;
frey; streak cherry-red, Qc : 37 silver, 41 antimony, 22 sulphur.
reiberg, Przibram, Potosi.
213. MoROCOCniTE (Silber-Wismuth Olaru), AgS-vBiS,,
Massive. Colour grey; streak light green. G. -6-92. C.c: silver
28 3, bismuth 547, sulphur 17. Morococha in Peru.
214. Sartorite, PbS-hAsjS,.
Eight prismatic Crystals slender; ooP 123° 20". CI. OP. H,-S;
G.-6-39. C.c: load 42-68, arsenic 80'93, sulphur 26'39. Binnen-
thal in Switzerland,
216. ZiNOKENITE, PbS-fSbSs.
Right prUmatic ooP (d) 120° 39'; foo (o) 150° 36' (fig. 349).
Crystals acicular ; vertically striated, and twinned
3 or 6. Sectile. H. -3 to 35; G.-5-3 to 5-35.
Steel-grey to lead-grey ; with blue tarnish. C.c: lead
35-9, antimony 42, sulphur 22-1. Wolfsberg.
216. Emflectite, CaS-^BiJS3.
Eight prismatic. Tin- white. Saxony, ■Wiirtcmberg,
and Copiapo.
217. WOLFSBEEGITE, Cu^S-hSbjSj.
Right prismatic ooP 135° 12'; oof 2 111°. Crystals tabular ;
also line granular. CI. brachydiagonal, perfect ; fracture conchoidal
or uneven. H. — 3 '5; G. = 4 '748. Lead-grey to iron-black, sometimes
iridescent; streak black, dull. C.c: 25'4 copper, 49 antimony,
and 25-6 sulphur, Wolfsberg.
218. Beethierite, FeS, SbSj.
Massive; columnar or_ fibrous, with indistinct cleavage. H. —
2-3; G.— 4 to 4-3. Dark steel-grey, reddish. Tintagel and Padstow
in Cornwall, Auvergne and Anglers (Creuse) in France, Braunsdorf io
Saxony. In France used as an ore of antimony.
219. Plagionite, Pb^Sbj.
Oblique prismatic, C 72° 28'. P 134° 30' and 142° 3'; -2P
120° 49 . Crystals thick, tabu_-
lar (fig. 350), minute, and in
druses. CL -2P, perfect; brittle.
H. = 2 -5 ; G. - 5 -4. Blackish
lead-grey. C.c: 41 lead, 38
antimony, and 21 sulphur.
Wolfsberg.
220. Klapeothite, SCu^S
•t- 2BL,S3 .
Eight prismatic; long striated
crystals; coP-107°. Wittichen,
Bulach. SchiTmerUe, from Colorado, 3(AgjPb)S + 2Bi2S» with O.
•=6-74, is similar.
221. BiNNiTE, 3CuS-l-2As,S3.
Cubic. Typical forms ooO, 202 ; 0, 00600 , 605 ; 404, lOOlO
303. H. -4-5 ; G. =4"48. Metallic. Black. Binnen.
222. JamesonUe, 3PbS H- 2Sb2S3 .
Eight prismatic; ooP 101° 20'. Crystals 00 P, ooPoo, long-
prismatic, parallel or radiating. CI. basal perfect, ooP and brachy-
diagonal imperfect; sectile. H. -2 to 2-5 ; G. -6-5 to 5-7. Steel-
grey to dark le^dgrey. B.B decrepitates, fuses easily, and wholly
volatilizes except a small slag. Sot in warm n. acid. C.c: 44-6
lead, with 2 to 4 iron, 34-9 antimony, and 20'6 sulphur. Cornwall,
Estremadura, Hungary, Siberia, and Brazil.
223. DCTFRENOrsITE, 2PbS-hASjS3.
Right prismatic. coP 93° 89'. Generally in thick rectongnlar
tables. H. -3; G. -5-66. Lead-grey. Brittle. Binnen, St Gotthard.
224. Feieslebenite, 5(Pb, Ag,)S -f 2SbjS3 .
Oblique prismatic, C 87° 48'. ooP 119° 12' ; P°
in prisms with curved reed-like faces, and
strong vertical striae. Twins intersecting ;
also massive. CI. ooP, perfect; fracture con-
choidal or uneven ; rather brittle. H. ■= 2 to
2-5 ; G. - 6-2 to 6-4. Steel-grey to dark lead-
grey. C.c: 22-5 silver, 32-4 lead, 26-8 anti-
mony, and 18-3 sulphur. Freiberg (Saxony), t
Hiendclacncina (Spain).
225. Pyeaegyrite, 3Ag,S-fSbjSj
Hexagonal rhombohedral ; R (/") 108° 42';
-JR137°68'; OR; -2R(r);R3; ooP2{s);
and 03R (;). Crystals prismatic (fig. 352);
twins common, of various kinds; also massive,
dendritic, or investing. CI. R, rather perfect;
fracture conchoidal to uneven and splintery; ''8- 3al (sp. A.4).
sectile. H. -2 to 26. Crimson-red to blackish lead-pey ; streak
cochineal to cherry-red. Huel Brothers and Hnef Duchy io
Cornwall, Andreasberg, Freiberg, Johaun-Geoi^nstadt, Annaberg,
Fig. 360 (sp. 219).
31° 41' (fig. 351)
MINERALOGY
395
Bchneeberg, Marienbsrg, Prnbram, Scliemnitz and Enmnitz,
Kongsberg, Mexico, Nevada, &c;.
226. PEOUCTrrE, 8Ag^+Aa,S,.
Bhombohcdra!, like pjTirgyrit!?, except R 107° £0' (flg. 858).
0.-S'6 to £-S. tloni-
tnuisptrtut to trans-
laoect oa the edges.
Cochir.sal to crimson-red.
C.c: 65-5 silver, 16"1
arsenic, and 19 '4 snlphnr.
Streak aurora-red. B.B.
araccisal. odour, and
difiicultly reduced to
metallic eilver. At the
same localities as pyrar-
gyrite; both are valu-
able ores of silver. Red
orpiment has a lower
specific gravity, and
yeUow streak; cinnabar
volatilizes before the -,. „,„ , „,. „.
blowpipe. ^*- ^^^ '^- ^^*- ^'8- 353 (sp. 226).
227. BOOLAKOEEITE, 8PbS-^SbS,.
Fine granular, columnar, radiating, or fibrous ; slightly seclile.
H. =3 ; G. — 6"8 to 6. Silky, metallic Blackish lead-groy, with
darker streak. B. B. like jamesonite. C. c. : 59 lead, 22 8 antimony,
a:id 18 ■ 2 sulphur. Moliires in France, Oberlahr (Rhenish
Prussia), Lapland, and Siberia. Plumbostib or EmbrethiU, fcora
Kertchuisk, is only a variety.
223. KoBELLiTB, 3PbS, BijSj-hSPbS, Sb,S,.
Radiated columnar ; soft G. - 6 "2 to 6 S. C. c. : 63 lead, 20 bis-
muth, 10 antimony, and 17 solphur. Hvena in Nerike (Sweden).
229. "WimcBisiTZ {Cuprams Sismuih), SCuS + BijSj.
Right nrismatic ; in tabular crystals like boumonite. 'Witticheo
in the Black Forest.
230. BoraNONiTE (3CuS-hSbjSj)4-2(3PbS+Sb,S,).
Bight prismatic ooP (<i) 93° 40'; ?oo(b) 96° 13'; P«j(0 92° 34';
DP (r); oo?oo(j); oofoo(i) (6g. 354). (3. brachydiagonal, im-
perfoct ; fracture uneven to conchoidal;
rather brittle. H. -25 to 3; G. = 67
to 5 '9. Lustre brilliant metallic. Steel-
grey. C.c. : 424 lead, 13 copper, 25
antimony, and 19*6 sulphur. Redruth
and Beeralaton ; Harz (Neudorf), Branns-
dorf, Eapnik, Servoz; Alais and Pontgi-
bond in France.
Wolchitt from Wolch in Carinthia is
only a variety.
231. AiKiNiTE {Needle-ore), 2(3PbS
J- BijS,) -H 3(CuS -^ BijSa).
Right prismatic ; long thin crystals
imbedded in quartz, often bent or broken; *
rather brittle. H. - 2 '5 ; G. = 6 7 to 6 -8. Fig- S»4 (sp. 230).
Blackish lead-grey or steel-grey, with a brownish tarnish. C.c. :
36 lead, 11 copper, 36 bismuth, and 17 sulphur. Berezoff (Siberia),
Georgia.
232. Sttlotyt, S(CuAgFe)S-HSbjS3.
Right prismatic OP 92° 80'. H.-=3;6.-4-8. Black. CoDiaTJO,
Chili.
233. AmnviTE, 4CuS-l-(AsjS3, SbjSj, BijSJ.
Massive, similar to the foregoing. From Anniver in Valais.
SlvderiU is similar, but with 15"5 of antimony.
234. JoLiANiTE, 3Cu2S-^AsJS,.
Cubic . G.-6-12. Metallic. Reddish grey. Eudelstadt in
Silesia.
235. Mbneohinite, 4PbS + Sb,S3.
Oblique prismatic, C 72° 8'. ooP 140° 24'; P°oo 70°. Crystals
small, acicular, chiefly of ojP* co , ooP°oo , ooP ; rare ; mostly
fibrous, H. -3: G. =6'4. Bottino in Tuscany, Schwarzenberg in
Saxony.
238. JOEDANITE, 4PbS-^AsA•
Right prismatic ; ooP 123° 29'. . CI. brachydiagonal, perfect.
Streak black. G.-6-88. C.c: lead 68-9, arsenic 12-5, sulphur
I8'6. Binuen and Kagyag.
237. Teteahedbite (FoAferz), 4Cu,S -f SbjS, .
■^.»0,
202
Tesseral and tetrahedral. In crystals -
355 to 358, also 65, 66, 206). Twins (iigs. 164, 207); generally
maf^ve. CL octahedral ; fracture conchoidal ; brittle. }£ ->3-44 ;
G.-4-6 to 6-2. St«5l-grey to iron-black; streak black (dark red
when containing zinc). B. B. on charcoal boils slightly, and fuses
to a steel-grey slag, usually magnetic, and with soda gives copper.
C.a aaBontially Cn^ in combination witli Sb^j. AirUirey near
Fig. 358.
Fig. 3S7.
Stirling, Sandlodge in Shetland, Tomnadashin on Loch Tay, Kirk-
cudbright; Crinnis and other Cornish mines near St Austell; Hai-z,
Miisen, Freiberg, Camsdorf, Alsace, Kremnitz, and Kapnik. Those
with 17 to 31 silver are the Silver Fahlare (Freiberg). Ore of
copper and silver.
238. TENKANriTE, (CuS, FeS) AsjSj.
Cubic (like fig. 237). CL ooO. Brittle. H. = 4; G. ~ 4 -3 to 4 5.
Iron-black ; streak dark red, grey. C.c. : 49 copper, 4 iron, 19
arsenic, and 28 sulphur. Redruth and St Day (Cornwall), and
Skutterud. Copper-blende, with brownish red streak; G. = 4 -3; con-
tains 8 '9 zinc ; Freiberg.
239. VoTSYTELUTE (Weissgiltigen), 4RS-^SbJS3.
Like tetrahedrita. H.-2-5;G. = 5-4to57. C.c: silver 6 to 22,
lead 38 to 52, antimony 85 to 22, sulphur 13 to 225. Freiberg.
240. Stbphamite, SAgjS-fSbjSj.
Right prismatic ooP (o) 115° 39'; P (P) middle edge 104° 20";
2foo(i) middle edge 107° 48'; OP (s); a>i<B(jo) (figs. 333, 334).
a. d and p, both imperfect ; fracture conchoidal or uneven ; sectile.
H. — 2 to 2-5 ; G. — 6'2 to 6-3. Iron-black to blackish lead-grey.
C.c. : 68'5 silver, 15'3 antimony, and 16'2 sulphur. Cornvrall,
Freiberg, Schneeberg, Annabcrg, Joachiinsthal, Przibram, Schem*
nitz, Mexico, Peru, and Sijjeria. Valuable ore of silver.
241. Geocronite, 5PbS-l-(Sb, As)5S3.
Right prismatic. Fracture conchoidal ; sectUe. H.=-2toS;G. -
6'45to6'54. Pale lead-grey. C. c : 67 lead, with 1 to 2 copper and
iron, 16 antimony, with 47 arsenic, and 17 sulphur. Sala in
Sweden, Meredo (Oviedo) in Spain, and near Pietrosanto in Tuscany.
242. KiLBRifczENiTE, 6PbS-^Sb~SJ.
Massive ; granular or foliated. C. c : 70 -01 lead, 1376 antimony,
and 16'23 sulphur. County Clare in Ireland.
243. PoLTE.vsiTE, 9(Ag2, Cn,)S-KSh, As}iS3.
Hexagonal ; P 117°. Crystals OP, coP ; and OP, P, tabular.
CI. basal, imperfect ; sectile, and easily fraacible. H. — 2 to 2'5;
G. -6 to 6-25. Iron-black, in very "thin lamellae, translucent,
red. C.c : 64 to 72 silver, 3 to 10 copper, IC to 17 sulphur, 02 to
8 antimony, and 1 to 6 arsenic. Freiberg,- Joachimstlial, Schem-
nitz, Guanajuato, Nevada, and Idaho. Rich oie of silver.
244. POLTARGTEITE, 12AgS -^ Sb.Sj .
Cubic. Typical form 0,ooO«>,<»0,mOm. Cl.cubic H.=2-5;
G. = 6-97. Metallic, iron-black ; streak black. Malleable. C.c:
782 silver, 7-4 antimony, 14-5 snlphur. Wolfach in Baden.
245. Enahgite, 3CUjS-f AsjSs.
Right prismatic. CL ooP 97° 53' perfect, brachvdiagonal 100° 68'
and jnacrodiagonal less so. Typical form eoP, OP, C«Poo, ooPto,
Brittle. H. -3; G. -4-3 to 4-5. Iron-black. C.c : 483 copper,
19*1 arsenic, aud 32-6 sulphnr, Uorococha in Peru.
.396
MINERALOGY
246. Olabite, 3CuS + AaS.
Obliijoo prismatic. CI. clinodiajonnl. Ordinary form oo >,
*eP'«>, OP, mP. II.— 0!>; C— 4'4d. Uark bliiiah grey. Kinzig-
thal in Baden. Luzor.ite ia Bimilar.
,247. Famatinite, SCuS + SbS.
Right prismatic. Typical form OP, ooP, <x.Poo, »p3. Massive or
reni/orm. H. -3-5 ; 0. -4-67. Copper-red to grey ; streak black.
Famatina Mts. in the Argentine Republic, and Cerro de Pasco in
Pern.
248. CniTiATiTE, aPbS + SBijS,.
Foliated, massive, 0.-6-9. Metallic. Lead-grey. Chiviato in
fern.
249. Epioenitb, eRS-hAsjSj.
Right prismatic. ooP 110° Btf. Steel-grey. H.-3-6. Witti-
Chen.
260. Epiboulanoerite, SPbS-FSbjSj.
Right prismatic. G. - 6 ' 3. Metallic. Blue-black, Altenburg
in Silesia.
251. Xantbocon, 2(3AgS-HA8jS3) + (3AgS-(-As2S5).
Hexagonal rhombohedral. R : OR 110° 30". Crystals thin hex-
agonal tables; brittle, easily frangible. H. -2 to 2-5; G. -5 to
5 '2. Translucent; adamantine. Orange-yellow or brown; streak
darker. In the closed tube fuses easily, becomes lead-grey. C.c. :
63'* silver, 14 '7 arsenic, and 21 '9 sulphur. Himmelsfiirst mine at
Freiberg.
252. Ptbostilpnite (Fire-blende).
Oblique prismatic ; crystals like stilbite. OP 139° 12'. Twins on
orthodiagonal. H = 2 ; G. = 4 -2. Lustre pearly, and adamantine.
Colour hyacinth-red and bright-yellow. Sectilo. C.c. : 62-3 silver,
with sulphur and antimony. Freiberg, Andrea^berg, Fr%ibram.
OXYSULPHURET&
253. Kekmesite, Sb03 + 2SbS3.
Oblique prismatic ; crystals ooPoo , OP, acicular and diverging;
sectile. H. - 1 to 1 -5 ; G. = 4 -5 to 4-6. Translucent ; adamantine.
Cherry-red ; streak similar. Sol. in h. acid. In potash solution
becomes yellow, and dissolves. C.c: 76'3 antimony, 19'8 sulphur,
4-9 oxygen. Braunsdorf, Przibram, Pernek near Bbsing (Hungary),
Allemont, Southham (Canada).
254. ToLTZiJffi, ZnO-t-4ZnS.
Incnisting. H. -•4-5; G. =-3 7. Yellow. Pontgibaud and
Joachims thai.
255. KAKELnoTE, 3BiO + BiS.
H. — 2; G. —e'S. Metallic. Lead-grey. Zavodinaki in the AltaL
156. BoLIviTE, BijOj + BLjSj.
Shombohedial. From Bolivia,
SELENITES.
357. Chaloomenite, CuSe + 2flj[=CuO, SeOj-f2HjO].
Oblique prismatic, C lOS" 20'. 6.-3^6. Bright blue. Trans-
•parent Co.: selenious acid 48-2, copper oxide 35'4, water 15-3.
Ccno de Cacheuta (Mendoza, Argentina Republic).
NITRATES AND BORATES.
258. NiTKATiNE, SajKj-NajO, NjOj].
Rhombohedral ; R. 106° 30'. Tarai^ca in Peru. Used in the
arts as a substitute tor nitre ; but deliquesces in moist air.
259. Nitre (SaZijKtre), KjKj:-K„0, NAl-
Right prismatic. 'SjP (^ 118° 49'; 2poo (P) 70° 65'; P«o 309° 62';
ooPoo(A) (fig. 276); isomorphous with aragonite. Acicular,
capillary, or pulverulent. CI. indistinct; fracture conchoidal. II. -
2 ; G. = 1 -9 to 2. Semitranspireut ; vitreous or silky. Colour-
less, white, or grey. Taste saline and cooling. Deflagrates
when placed on hot charcoal ; .and B.B. on platiua wire melts very
easily, colouring the flame violet. C. c. : 46 -6 pot.vsh and 63 i nitric
acid, but always more or less impure. In tlio limestone caves of
many countries; Hungary, Spain, India. Used for producing nitric
acid, in glass making, medicine, and the manufacture of gunpowder,
260. NiTROOALCITE, CaiS'j-Hllj.
Fil'rous or pulverulent. ^V^lito or grey. C.c: 30-8 lime, 69-3
nitric acid, and 9-9 water. Limestone caves of Kentucky ; on old
walls and limestone rocks.
261. NiTROMAONESITB, Mg>I\-|-lI;.
Taste bitter. luHic same places, and similar to iiitrocalcite.
262. BoEACiTE, 2MgjBj + MgCl.
Tesseral and hemihedral (figs. 63, 253, 359). CL octahedral, im.
Serfect ; fracture conchoidal ; brittle.
[.-7; G. -2-9 to 3. Transparent or
translucent ; vitreous or adamantine.
Colourless or while, often greyish, yellow-
ish, or greenish. Becomes polar electric by
heat. B.B. fuses with diiculty to a clear
yellowish bead, which on cooling forms a
white opaque mass of needle-like crystals ;
at the same time colours the flame green.
Sol. in h. acid. C.c. : 62 '6 boracic acid,
269 magnesia, 7'9 chlorine, and 27 mag-
nesium. Liineberg, Segeberg in Holstein, Fig. 359.
Stassfurt.
263. Stassfjtrtite.
In very minute prismatic crystals. "Wliite. C.c. same as bora-
cite, and thus perhaps dimorphous. Stassfurt.
264. Khodizite, 2(ia,'B, (?).
H. — 8 and G. =3'3 to 3 '42; agrees in most characters with
boracite. Pyro-electric. Mursinsk in Siberia.
255. LUBWIGITE, 21rIg'fii-HFe!Fe2.
Fibrous masses. From limestone at Morawitza in the Banat.
266. BoKAX(7'intaZ), S'a„2B + 10ft,.
Oblique prismatic, C 73° 25'. ooP 87° ; P 122° 34' (fig. 360).
Almost isomorphous with augite; brittle. H. =2
to2-5;G.-17tol-8. Pellucid; rerinous. Colour-
less, or yellowish, greenish, and greyish white.
Taste feebly alkaline and sweetish. C.c: 16'4
soda, 36 '5 boracic acid, and 47 '1 water ; but often
with 2 phosphoric acid or other impurities. Shores
of salt lakes in Tibet and Nepal, in California,
and near Potosi.
267. Borocalcite, (;a2B -H 6ft. ,
Similar to ulexite (sp. 268) ; and from same ^
locality.
268. Ulexite, l>fa52'B-(-2Ca2B + 18Hj.
Fibrous. H. =1 ; G. — 1 -e. AVhite. Tasteless. Iquique and Nov;i
Scotia.
"^69. SzAIBELTITE, 2Mg52'B + 3H3.
H. -3-5 ; G. -27. WerksthSl in Hungary.
270. Htdroboracite, 2(5a3B3-l-2]ifg3l53-Hl2llj.
Radiating and foliated. Caucasus. A similar mineral, with soda
ia place of magnesia, is found in Peru.
271. Scssexite, (Mn, Mg).B + Hj.
Fibrous, silky. White H. = 3;G. = 3-4. Franklin (Sussex
county. New Jersey).
ANHYDROUS CARBONATES.
272. Caloite (Calc-spar, Calcareoiis Spar), (5aC.
Hexagonal and rhombohedral ; R 105° 5' (fig. 101). The forms
and combinations exceed those of any other mineral. Among them
are more than fifty rhombohedrons, especially - ^R 135° ; R ; - 2R
79° ; and 4R 66° ; with OR and ooK as limiting forms. There aro
one hundred and fifty-five distinct scalenoliedrous, as R3 ; R2 ;
|K3 ; and the second hexagonal prism ooPS. Hexagonal pyramids
are among the rarer forms. Some of the most usual combinations are
ooR, -iU(c, ff, fig. 179); or -JR, aR, very frequout ; also ooR,
OR ; likewise -2R, R if, P, fig. 107) ; K3, t»E, - 2R ; R5 (y), R3
(r), R (P), 4R (m), ooR (c) (fig. 109); R, R3 (fig. 108). Several
' undrcd distinct combinations aro known.
Hemitropes and twins aro not uncommon. These occnr
with the axes parallel (figs. 106, 146, 148, 180, 366, 367). Othen
Fig. 360(sp. 266X
Fig. 361. Fig. 362. Fig. 363. Fig. 364.
are conjoined bv a face of R, the axes being .ilmost at right angles,
89° 8' (figs. 183, 369) or by a face of - 4R, in which the chief
axes form an angle of 127^°; and usually many times repeated,
so that the centre crystals appoar in lamclhc not thicker than
paper (fig. 161) ; at an obtuse angle, as figs. 149, 363, or an acute
MINERALOGY
397
angle, as fi^ S64, 368. Also occurs grairalar, lamellar, parallel
or radiated fibrons, compact and earthy. CL rhombohedral along
R, Tery pcrfoct and easily obtained, so that the conchoidal
fracture Li rarely observable; brittle. H. -3 ; G. -2-6 to 2'8 ; pure
truupaient crystals — 272. Pelluoid iu all
degrees. Very distinct double refraction.
Lnstre yitreous, but several faces 'rerinous, and
OR pearly. Most frequently colourless pr
white, but often grey, blue, green, yellow,
red, brown, or black ; streak greyish white.
B. B. infusible, but becomes caustic and emits
a bright light.' Effervesces, and ia entirely
8cL in h. or n. acid. The fine powder, ignited ,j.,
on platina-foil over the spirit-lamp, forma a ^* ^^
somewhat connected mass, and even adheres to the platina, Co.
of the purest varieties, carbonate of lime, with 41 carbonic acid and
66 lime, but usually contains magnesia and protoxide of iron or
of manganese. Remarkable specimens of the crystallised variety
or proper calc-spar are found at Alston
Uoor in Cumberland (Sat rhombic
crystals) and iu Derbyshire (pale yellow
Kit- 36a Fig. 367.
transparent pyramids), at Strontian, Elie in Fife (figs. 370, 871,
372), Andreasberg and other parts «f the Harz (six-sided prisms),
and at Freiberg, Tharand, and Haxen iu Saxony.
Certain vanetiea are distinguished. Iceland Spar, remarkable
lor its transparency and double re-
fraction, occurs massive and in huge
crystals in a trap rock in Iceland.
Slatt Spar, thin lamellar, often
..with a shining white pearly lustre
and greasy feel; Abergaim and Glen
I c i<^ e I
Fig. 368. " ?ig. 369.
Tilt In Scotland, Wicklow in Ireland, and Norway. AphrUe, fine
scaly ; from Hesse and Thuringia. Marble is tne massive crys-
talline variety of this mineral, produced by igneous action on com-
pact limestone. Faros, Naxos, and
Tenedos furnished the chief supply to
the Grecian artists ; Carrara, near the
Gulf of Genoa, to those of modem
times. Some of the coloured marbles
Fig. S7a Fig. 371.
«i the ancients were impure Umestonu, as the CipoUino, zoned
with green talc or chlorite and Verde Arttique, mixed with green
Fig. 372.
serpentine. Ruin Marble shows irregnlar markings like rvina;
Val d'Amo (Florentine marble), and Bristol (Qjtham marble)
LueulliU from Egypt, and ArUhraamite, from Campbelltown and
Kilkenny, are black from carbon. L-umachdlo, from Bleibcrg in
Carinthia, exhibits beautiful iridescent colours {rom fossil shells,
sometimes deep red or orange (Fire Marble). Bislopite, £rom
Poonah, is green, from celadonite.
Limestone occurs in all formations under various names, as OoltU,
e^-stone, or roe-stone, — round concretioiiawithaconccntricstructur*
like the roe of a fish ; Pisolite, or peastone,
siicilar structure ; CTialk, ' soft earthy ;
Lithographic Stone, yellowish and compact,
from Solenhofen ; and Marl, calcareous
matter more or less mixed with clay.
Calcareous Tufa, generally a recent deposit
from calcareous springs, has often a loose
friable texture, but at other times is hard
and compact; and in the neighbourhood of
Rome forms the common Duilding stone
Travertine. The sandstone of Fontaine-
bleau is carbonate of lime (i) mixed with
quartz sand (|), and occasionally crystal-
lizing iu thombohedrons.
TUs mineral is employed in many
ways! — the coarser varieties, when burnt
to drive off the carbonic acid, as lime, for
mortar, manure, tanning ; as a flux in
melting iron and other ores, or in pre-
paring glass, and for similar purposes ; the
finer, as marbles, for sculpture, architec-
ture, and ornamental stone-work ; the chalk for writing, white-
washing, or producing carbonic acid.
Flumiocalcile. — CI. 104° 63'. White and pearly ; softer than
calc-spar ; but G. — 2'824. Contains 2 '3 to 7 "8 carbonate of lead.
Wanlockbead and Leadhills (Scotland).
273. Dolomite {Bitter-spar), CaO-l-Mgd.
Hexagonal rhombohedral ; R 106° 15'-20' ; most frequent form
R. The rhombohedrons often curved and saddle-shaped ; also
granular or compact, often cellular and porous. CL rhombohedral.
fl. -3-5 to 4'5; G. -2-85 to 2 95. Translucent; vitreous, but
often pearly. Colourless or white, but frequently pale red, yellow,
or green. B.B. infusible, but becomes caustic, and often showa
traces of iron and manganese. Fragments effervesce very slightly
or not at all in hydrochloric acid ; the powder is partially soluble,
or wholly when heated. C.c: 64 '3 carbonate of lime and 46 T
carbonate of magnesia, but generally carbonate of lime with more
than 20 per cent carbonate of magnesia and less than 20 per cent,
carbonate of iron.
Varieties are — Dolomite, massive-granular, easily divisible, white;
Rhomi or Bitter-epar, larger grained, or distinctly crystellized and
cleavable, often inclining to green ; and Brovm-spar and Pearl-spar,
in simple crystals generally curved (fig. 231), or iu imitetive forms,
of colours inclining to red or brown, more distinct pearly lustre, and
under 10 per cent, carbonate of iron. Leadhills and Charlestown
in Scotland, Alston in Cumberland, in Derbyshire, Traversella in
Piedmont, St Qotthard, Gap in France. Greenish, twinned ; Miemo
in Tuscany (Miemiie), and Tharand in Saxony (Tharandiie).
The massive and compact varieties are very common, and are
valued as building stones (cathedral of Milan, York Minster, and the-
Houses of Parliament at Westminster). The Parian marble, and
also the Sutherland and lona marbles, belong to this species.
274. AifKEEiTE, CaC■^(S^gfe)0.
R 106° 12". Usually massive and grannlar. Q. -2-9to$'l.
Otherwise like siderite. Unst (Shetland), Styria.
276. Maonzsite, Mg(3.
Rhombohedral ; 107* lO'-SC. Reniform or massive, H. -36;.
G. — 2'86 to 2 '95. Subtranslncent or opaqne ; streak shining.
Snow-white, greyish or yellowish white, and pale yellow. Tyrol,
Norway, North America.
276. BREOTTNEErrE (ffwiertife), Mg6-t-(lilnf'e)C.
Hexagonal rhombohedral; R 107° 10'-30'. Granular or columnar.
CL R, very perfect H.-4to4'5; G. -2'9to3'l. Transparent or
translucent on the edges ; highly vitreous. Colourless, but often
yellowish brown or blackish grey. C.c. essentially carbonate of
magnesia, with 51 '7 carbonic acid and 48 '3 magnesia, but often
mixed with 8 to 17 carbonate of iron or manganese. Unat, Tyrol (in
Fassa Valley, &c), St Gotthard, Harz.
277. Siderite (Sj>arry Iron, Chalybite), FeC .
Hexagonal and rhombohedral ; R 107°. Chiefly R, often curved,
saddle-shaped (fig. 232), or lenticular. CL rhombohedral along R,
perfect; bnttle. H. -3'5 to 4'5 ; G. -3'7 to 3'9. Tranalncent in
various degrees, becoming opaque when weathered; vitreous »r pearly.
'R-arely white, generally yellowish grey or yellowish brown, changing,
398
MINEKALOGY
to red or blackish brown on exposure. B.B. infusible, bnt becomes
black and magnetic ; with botai and salt of phosphoras shows
reaction for irou ; with soda often for manganese. In acids soluble
with effervescence. C.c. carbonate of iron, with 62 1 protoiide of
iron and 37 5 carbonic acid, but nsuaUy 0 5 to 30 or even 25
piotoiidi. 01 nwnganoso, 0-2 to 15 magnesia, and O'l to 2 lima.
Unst, iantyre. In beds or masses in Boeralston in Devonshire,
Alston Moor m Cumberland, and in many of the tin-mines in
Cornwall m Styna, Carinthia, end WestphaUa ; in veins in Anhalt
andtheHarz; also in the Pyrenees and the Basque provinces of
^8in, as near Bilboa ; in crystals at Joachirastha; Freiberg,
t F^^ Irmstpne, grey, blue, brown, or black,— G. - 2 -8 to 3 -5, H. -
S'o to 4 '5, — is an impure variety.
278. DiALOGiTE {Kcd Manganese), MnC.
Hexagonal rhombohedral ; R 106° 56'. Crystals often curved,
lenticular, or saddle-shaped ; also spherical, reuiform, and columnar
or granular. CI. R, perlcct. H. - 3 '5 to 4 -5 ; G. - 3 -3 to 3 -6. Trans-
lucent ; vitreous or pearly. Rose-red to flesh-red ; streak white.
C.c: 62 manganese protoxide and 38 carbonic acid. Freiberg,
Schemnitz, Kapnik, Kagyag, Elbingerode, and near Sargans
279. COBALTSPATH, CoCo .
Rhombohedral and spheroidal. H. -4 ; G. =4 to 4-13. Peach-
blossom-red ; but dark externally. Schneeberg.
280. Smithsonite {Calamine), ZnC .
Hexagonal rhombohedral ; R 107° 40'. Usually renifonn, stal-
aotitic, and laminar or granular. CI, R, perfect, but curved; fracture
uneven, conchoidal ; brittle. H. - 6 ; G. =4-1 to 4-5. Translucent
or opaque ; pearly or vitreous. Colourless, but often pale greyish
yellow, brown, or green. C.c: 64 8 zinc oxide and 35-2 carbonic
acid. Mendip in Somersetshire, Matlock in Derbyshire, compact at
Alston Moor, Chessy near Lyons, Altenherg near Aix-la-Chapelle,
Brilon in Westphalia, Tamowitz in Silesia, Hungary, Siberia.
281. Akaoonite, CaC.
Eight prismatic. ooP116°10' ; P<d 108°26'. The most common
combinations are a,f<a (h), oof (J/), Poj (i, P) (fig. 275), generally
long prismatic (like the separate crystals in fig. 184)
OP, generally short prismatic ; crystals of 6P4, coP, f.
(fig. 373) acute pyramidal. But simple crystals are
rare, from the great tendency to form twins, con-
joined by a face of ooP, and repeated either in
linear arrangement (fig. 185) or in rosette group-
ing (fig. 186). Also columnar, fibrous, and in
crusts, stalactites, and other forms. CL brachy-
diagonal, distinct ; fracture conchoidal or uneven.
H. = 3-5 to 4 ; G. -2-9 to 3 (massive 27). Trans-
parent or translucent ; vitreous. Colourless, but
yellowish white to brick-red ; also light green,
violet-blue, or grey. In the closed tube, before
reaching a red heat, it sweUs, and falls down iuto
a white coarse powder, evolving a little water.
Unst and Lcadhills ; Valencia, Molina and else-
where in Aragon ; Leogang in Salzburg, and Anti-
paros. Flos-ferri, coralloid, in the iron-mines of
Styria. Satin-spar, fine fibrous silky, at Dufton
(Westmoreland). Stalactitic, coast of Galloway,
Leadhills, Buckinghamshire, and Devonshire. Also
deposited as tufa by the Carlsbad and other hot
pprings.
282. WiTHERITK, fiaC.
Eight prismatic ooP (j) 118° 30'; 2?oo(P) 112°. Crystals
not common like fig. 275, but generally with quite an hexagonal
aspect from being twinned like aragonite
(fig. 374). Of tenor spherical botryoidal, or
reniform,with radiated-columnar structure.
CI. 00 P, distinct ; fracture uneven. H. — 3
to 8"5 ; G. — 4'2 to 4'3. Seraitransparent
or translucent ; vitreous, or resinous on
the fracture. Colourless, but generally
yellowish or greyish. B.B. fuses easily
to a transparent globule, opaque when
cold ; on ciiarcoal boils, becomes caustic
and sinks into the support ; soluble with
cfiervescence in n. or h. acid. C.c: 22'3
carbonic acid and 77'7 barj'ta. Alston
Moor and Hexham in Northumberland,
also in Styria, Salzburg, Hungary, Sicily
Siberia, and Chili.
Fig. 373.
Fig. 374.
283. Alstonite, feaC-l-dlaO.
Right prismatic ooP 118° 60'; 2f oo 111° 60' ; usual combination
', 2P<o, ooP, resembling an hexagonal pyramid (fig. 375). CL ooP
4 to 4 ; ■ 0. -.^UB 1? 3-r«.
Fig. 375 (sp. 28-3).
and 00 Poo, rather distinct H. —
376. Translucent ; weak resinous.
Colourless or greyish-white. C.c:
66 carbonate of baryta and 34
carbonate of lime. Fallowfield near
Hexham, and Alston Moor.
284. Steontiakite, SrC.
Right prismatic o»P 117° 19';
?co 108° 12'. Crystals (fig. 376)
and twins like aragonits ; :dso broad
columnar and- fibrous. CI. pris-
matic along ojP (il). H. -8-£;
G. -3-6 to 3-8. Translucent or
transparent ; vitreous or resinons
on fracture. Colourless, but often
light asparagus- or apple-green, more
rarely greyish, yellowish, or brown-
ish. B;B. fuses in a strong heat
only on very thin edges, intumesccs
in cauliflower-like forms, shines
brightly, and colours the flame red : easily soluble in acids, with
eS^ervescence. i: 30 carbonic acid and 70 strontia. but often
contamsc--' (of lime (6 to 8).
Stron .. .tvrgyllshire, Suther-
land, 1 -ogang in Salzburg, Brauns.
dorf in Saxony, Hamm in West-
phalia, the Harz; at Schoharie
(N.Y.) and elsewhere in United
States (Emmonite). It is nsed
to produce red fire in pyrotechnic
exhibitions. f jg. 376.
285. Manganocaioite, (Sin, Oa, te) C .
Right prismatic ; in prisms like aragonite, and bears the samo
relation to dialogite that aragonite does to calc-spar. H. — 4 to 6 ;
G. = 3'03. Red or reddish white. Titreoua. Schemnitz.
286. Ceeussite (Lead Spar), PbC .
Right prismatic; isomorphous with aragonite and nitre. wP
{M) 117° 14'; P« 108° 16'; 2foo (u) C9° 20';
also OP; P (t); J-Poo (s); cc?oo {I); afs (f)
(fig 377). Twins common (figs. 158, 169, 378,
379). Also gianular or earthy. CI. ooP and
2Pa: , rather distinct ; fracture conchoidal ;
easily frangible. H. -3 to 3-5; G. -6-4 to
G'Q. Transparent or translucent ; adamantine
or resinous. Colourless and often white, bnt
also grey, yellow, brown, black, rarely green,
blue, or red ; streak white. B. B. decrepitates
violently, but easily fused and reduced ;
soluble with effervescence in n. acid. C.c .
83 '5 protoxide of lead and 16 '5 carbonic acid.
Very common. Leadhills, Wanlockhead,
Keswick, Alston Moor, Beeralston in Devon-
shire, St Minver in Cornwall ; Przibram. Mies, and Bleistadt ;
Fig. 377."
Fig. 378. Fig. 879.
Tamowitz, Johann-Georgenstadt, Zellerfold, Elaustbal, and m&oy
other places.
287. Babyto-Caloite, fiaC-fCaO.
Fig. 880. Fig. 381.
Oblique prismatic, C 69* 80'. ,ooP (m) 84* 62", P (») 108* 64',
MINERALOGY
399
Fig. 882 (sp. 289).
22 Boda, 16 carbonic
^
Fig. 383.
F°oo (1)61* (figs. 880, 881); also colamnar and granular. C^ P
perfect, P"") leas perfect. H. -4; G. -3-6 to 8-7. Transparent
or translucent ; vitreous, inclimng to resiaoos. Yellowish white.
Co. : like alstonite. Alston Moor.
288. BiSMUTO-SPBUSBITE, BijO .
Small fibrous brown concretions from Keustadtel, near Schnee-
beig.
HYDROUS CARBONATES.
289. Tesbuonatbite, ifci,G + ^.
Eight prismatic. o.p2 (d) 107° 50'; f oo (o) 83* 60"; with a,fa>
(F) in rectangular tables (fig. 382). CI.
brachydiagonal, perfect. H. = 1'5;G. — IS
to 1*6. Colourless. D. B. like natron,
but does not melt. C.c. : SO °1 soda, 86 '4
carbonic acid, and 11 'S water. Natron
lakes of Lagunilla in Venezuelp, of Lower
Egypt, and of the steppes between Urals
and Alt&i.
290. Natbon, ifa^C + lOfl,.
Oblique prismatic, C 57° 40'. Crystals"
artificial ; with ooP 79° 41' ; P 76* 28'.
CL orthodiagonal, distinct. H. »ltol'6;
O. — 1 4 to 1 '6. Pellucid ; vitreous.
Colourless or greyish white. B.B. melts
easily, colouring the Same yellow. C.c
acid, and 63 water ; but mized with chloride of sodium and oth^
salts. Only as an efflorescence on the ground or rocks (lava of
VesuTJus and Etna) in various countries (Hungary, Egypt, Tartary),
and in mineral springs and lakes. Used in the manufacture of
soap, in dyeing, and in bleaching.
291. Teona, Ubao, NajCj+lSj.
Oblique prismatic. Crystals OP (T), ooP«oo (if), P (n). T:M
103° 16' (Bg. 383). CI. orthodiagonal, perfect.
H.-2-6 to 3; G. -2-1 to 2 2. 'Transparent to
translucent. Colourless. Does not decompose is
the air. Taste alkaline. C.c. : 38 soda, 40 car-
bonic acid, and 22 water. Fezzan and Barbary
[Trona), Lagunilla (CTi-oo).
292. Gatlcssite, iJajO + Ca(3 + Sfi, .
Oblique prismatic, 0 78° 27'. CL <»P, imperfect ; fracture
oonchoidaL H. — 2'6; G. — 1'9 to 1'95. 'Transparent; vitreous.
Colourless. C.c. : 34 '6 carbonate of soda, 33 '6 carbonate of lime,
30 -4 water, with 1'6 clay. Lagunilla.
293. HYDKOSIAQNEaiTE, Mg^C, + 4Sj ..
Oblique prismatic. ooP 88° nearly. Crystals small, rare ; also
massive. H. -IS to 3; G. -214 .to 218. Vitreous or silky.
VThite. C.c. : 36'2 carbonic acid, 44 magnesia, and 198 water.
0nst (Shetland), Moravia, Kumi in Negropont, Hoboken in New
Jersey, and Texas in Pennsylvania.
294. AzDEiTE {Blue Copper), (5u,C,+ ll,.
Oblique prismatic, C 87° 39'. ooP {M) 99° 32*; - P (if) 106° 14'.
Crystals OP, o.P, oopooo , - R (or A, M, s, ii, in fig. 384, but in
another position) ; also radiated and earthy. CI. clinodomatic {P)
69° 14', rather perfect ; frac-
ture conchoidal or splintery.
H.-S-6to4-2; 0.-37 to 38.
Translucent or opaque ; vitre-
ous. Azure-blue, the earthy
varieties (and streak) smalt-
blue. B.B. on charcoal fuses
and yields a grain of copper ;
Boluble with effervesceuce in
acids, and also in ammonia.
Co.: 69 1 protoxide of copper. Fig. 384.
25'7 carbonic acid, and 6-2 water. Crestals at Redruth, Alston
Moor, Chessy near Lyons, in Siberia, Moldawa in the Banat, Burra-
Barra (Australia). Valued as an ore of coppen
; 295. Malachite, Cu^C + Hj.
\ Oblique prismatic, C 01° 60'. ooP 104° 20'. Crystals ooP {M),
<»P°oo (j), OP (P), in hemitropcs (fig. 385). In general acicular,
scaly, or reniform, stalaotitic, end radiated fibrous.
CL basal and clinodiagonal, very perfect. H. - 3 '5
to 4 ; G. —3 '6 to 4. Transparent or translucent on
the edges ; adamantine, vitreous, silky, or dull.
Emerald and other shades of green ; streak apple-
wen. B.B. and with acids like azurite. C.c. :
71 '8 copper protoxide (- 67 S copper), 20 carbonic
acid, and 8 2 water. Crystalline at Rheinbreiten- — ~
bach on the Rhine and Zellerfeld in the Harz ; fibrous Fig- 385.
and compact at Sandlodge in Shetland, LeadhiUs, Cornwall, Wales,
and Iieland, at Cheasy ia Fiance, Siberia, the Uisls, Ssalfeld m
Thuringia, Moldawa in the Banat, in North America, Africa, and
Australia. Frequently pseudomorphous after copper and its ores,
also after calcite and cerussite. Valuable ore of copper ; the finer
varieties are prized for ornamental pui-poses.
296. Htdeozinoite, ZnC + 2Znfi, .
Massive. Co. : zinc oxide 753, carbonic acid 18'6, water ll'L
Spain, Westphalia, Bavaria, Persia, United States, Valuable ore.
297. AtJBioHALorrE, 2CuO + SZnfl,.
Acicular. H. =2. Translucent, pearly, and verdigris-gnen.
C.c: 29 2 copper protoxide, 447 zinc oxide, 16'2 carbonio add,
and 9*9 water. .LeadhiUs, Matlock, Loktevski in the Altat
298. Emeeald-Niokel [ZaratUe), ^10 + 663.
Amorphous, reniform, and incrusting. H. -^3; G.— 2*6 to 27.
Translucent; vitreous. Emerald-green. C.c: 59 '3 nickel pro-
toxide, 117 carbonic acid, and 29 water. On chromite at Hsgdale
in Unst, 'Texas in Pennsylvania ; also Cape Ortegal in Spain,
Tyrol, and Ekaterinburg in the Urals.
299. LiNDAKERITE, U,C+ 2C;aO-h lOflj.
In small siskin-green crystalline aggregates, H.— 2'6 to 8.
From Elias mine near Joachimsthal, implanted on pitcU-blende.
300. VooLiTE, 4Ufi-^7(5aC-^3(!;a(j + 24Il,.
RhomboidaL Emerald-green scales with pearly lostre. Eliai
mine, Joachimsthal.
301. LiEBiotTE, tJ■JS-l-(5aC■^20fi,.
Mammillary concretions. H. =2 to 2 '6. Apple-green. Adrian-
ople, Joachimsthal, and Johann-Georgenstadt.
302. BiSMUTHITE, Bi<C,-K411j.
Disseminated, investing or acicular; fracture conchoidal or nn-
even ; very brittle. H. =4 to 4-5 ; G. -68 to 691. Opaque ; dull
vitreous. Grey, yellow, or green. C.c. : 90'1 bismuth oxide, 6'4
carbonio acid, and 3 '6 water. Ullersreuth (Reuss), Schneeberg,
Johann-Georgenstadt ; also Chesterfield in South Carolina.
303. Lanthanite, LaC-hSflj.
Right prismatic. oaP 92° 46'. Small tabular crystals ; nsuallj
granular or earthy. CI. basaL H. - 2 ; G. - 27. Dull or pearly.
vVhite or yellowish. C.c. : 21 carbonic acid, 55 lanthanum ozide^
and 24 water. Bastnaes in Sweden, Lehigh in Pennsylvania.
CARBONATES WITH HALOID SALTS, ho.
304. Phosoenite, PbCl-hPbii.
PyramidaL P 113° 56'. Crystals short-prismatio or sharp'
pyramidal. CI. ooP, rather perfect ; f.'octuro
conchoidal. H. -2-5 to 3; G.-6 to 6 2.
Transparent or translucent ; resinous adaman- 1
tine. White, yellow, green, or grey. C.
61 chloride and 49 carbonate of lead. Very ]
rare. Stottfield 1
n(^r Elgin
Scotland, Matlock [
and Cromford in
Derbyshire, Tar-
nowitz. Fig- 886.
306. PASurrs, SCeC-fCaP.
Hexagonal. P 164° 68'. CL basal,
perfect. H. -4-5; G. -4-35. Vitre-
ous ; on cleavage - plane pearly.
Brownish yellow, inclining to red.
C.c. : 23 '6 carbonic acid, 42 '5 prot-
pjo- ^S7 /■cTi ^Cif.\ oxide of ; cerium, 8 "2 lanthanum
rig. Ml ^6p. ouoj. ^^^^^ g.g ^jy^„nj o^4g^ 2-8 Ume,
lO'l fluoride of calcium, and 22 fluoride of cerium,
mines of the Muiio Valley in Colombia, Urals.
306. LEADHiixiTE(3/iza;f««), PbijCi^jOiij-f-Sll,.
Right prismatic. P middle edge 187°; ooP 120° 20'; 2t
Emerald
Fig. 388.
Fig. 389.
Mostly tabular ; also twins. CL basal, perfect ; slightly brittle.
H. -2'6 ; G. -6-26 to 6 '44. Transpaient or tnuulucent ; reeinoui
400
MINERALOGY
Fig. 391 (sp. 307).
or adain.inti:io, pparly on OP. Yellowish white, inclining to grey,
green, j-cllow, or brown. C.c. : 81 98 oxide of lead, 803 car-
bonic acid, 8'12 sulphuric
acid, 1"8 water. Lead-
hills, Taunton, Neftchinsk,
Granada. Maxitt from Sar-
dinia.
307. ScsAN.viTE, 8tbC
-t-fbS.
Rhombohedral ; R 72°
29'. CL basal, perfect.
H. -2-5; G. -6-65. White,
j;reen, yellow, brownish.
Resinoua to adamantine ;
pearly on the cleavage
faces. Powder white.
C.c: 72 '6 carbonate and
27 '6 sulphate of lead.
From the Susanna mine at „. „.. , „ „„,
LeadhiUs, but Tory rare ; "^S- ^^^ ''?• 2<"'
also in large dark crystals from the Banat.
ANHYDROUS SULPHATES.
803. Aeoanite (OlaseriU), fejS .
Right prismatic Acute pyramids, with ooP 120° 24'; dimorphous
and also rhombohedral, with R 88° 14'. Mostly in crusts, or pul-
Temlent. OL basal, imperfect. H. -2-5 to 3 ; G, =27. Pellucid;
vitreous or resinous. Colourless or white. C.c. : 54 potash and 40
sulphuric acid. Lavas of Vesuvius and other volcanoes,
309. .Masoaonine, (Nli,)^'.
Right prismatic. ooP 121° 8' ; but chiefly in crusts and stalac-
tites. CI. perfect; sectile. H.-2 to 2-6 ; G. = 17 to 1-8. Pel-
lucid ; vitreous. Colourless, white, or yellowish. Taste pungent
and bitter. C.c. : 25'9 ammonia, 60"5 sulphuric acid, and 13'fl
water. Near volcanoes, as Etna, Vesuvius, the Solfatara, the
Lipan Islands, in the marshes near Siena, and in ignitod coal-beds,
as at Bradley in Staffordshire.
310. Thenardite, Naj's.
Right prismatic. Acute pyramids P, with OP and ooP, in crusts
and druses. CI. basal, perfect; fracture uneven. H. — 2"5; G. =
2-6 to 2 7. Pellucid; vitreous. White. C.c. : 43 82 soda and
66*18 ^Iphuric acid. In salt deposits near Aranjuez (Spain) and
at Tarapaca (Peru).
311. Glauberitb (^roTi^iortmi!), Na^S+fca'S'.
Oblique prismatic, C 68° 16'. OP, - P, or with ooP (P, /, M,
392). CL basal, perfect; along c«P traces. H.-2-5
to 3; 0.-275 to 285. Translucent; vitreous to
resinous. Colourless. C.c. : 51 sulphate of soda,
and 49 sulphate of lime. Villarnbia in Spain, Vic,
Berchtesgaden, near Brugg in Aargau, Aussee and
Ischl in Austria ; Tarapaca in Peru, with I to 5
boracic acid.
312. Anhydrite (KarslmiU), CnS.
Right prismatic. ooP 90° 4'. Chiefly granular, or almost com-
jvact or columnar. Twins rare. CI. macrodiagonal and brachy-
diagonal, both perfect; basal perfect. H.— 3 to 3'6 ; G.-2'8 to
3. Transparent or translucent ; vitreons ; on odPoo pearly.
Colourless or white, but often blue, red, or grey ; streak greyish
white. C.c. : 58 75 sulphuric acid and 41 '25 lime.
The crystalline, or MiiriaciU, occurs in the salt-mines of Bex, Hall
in Tyrol, and Aussee in Styria, also at Sulz, Stassfiirt, and Bleiberg.
Compact at Isclil in Austria, Berchtesgaden, Eisleben, and the
Harz. Granular, or Vnlpinite, near Bergamo. The contorted, or
OtkrHsstein, chiefly at Wieliczka and Bochuiu.
313. B.vryte (iTcary 5p(ir), fiaS'.
Right prismatic P=o (3) 78° 20"; Pco (/) 105° 22'; <xf2 (d) 77°
ii! ; also ooPoo (c) (figs. 125, 126, 127, but in a different position,
d,*d being placed vertical). The crystals show very many forms
and combioatiouB, and aro tabular or columnar, often in druses or
groups; also foliated, fibrous, granular, or compact. Ci. biacliy-
diagonal peifect, along fao less perfect; basal, traces. II. -3
to 35; G.— 4 3 to 47. Transparent to translucent; vitreous
or resinous. Colourless and white, but generally reddish wliite,
or flesh-red, yellow, grey, bluish, grcenisli, or brown. B. B.
Jc<ropitat«3 violently, ana fuses vciy diUieuUly, or only on the
vdgcs, colouring the flame yellowisli green ; not soluble in acids.
C.c. : 343 sulphuric acid and 657 borjta, but occasionally
>vilh 1 to 15 sulpliato of strontia. Very common, chiefly iu veins,
either alone or accompanying ores. Crystals at Arran, Strontian,
Elie, Sutherland ; Dufton, Bohemia, Felsobanya and Kxemiit* iu
Fig 392
Hungary, Auvcrgne, and United States. Colnmnar at Freiberg.'
The radiatid from near Bologna, or the Bolognest Stone, phos-
phoresces in the dark. Massive, or Cawk, from Derbyshire and
Staffordshire, Leadhills, and Arran. ,- *^, . *
Lime Baryta, from Derbyshire, Strontian, Freiberg, seems a
mixture with sulphate of lime ; crj-stals tabular, in rosettes and
other groups; G. -4 to 4 3. Hepatite, dark grey, from carbona-
ceous matter ; Kongsberg. AllovwrvhiU, scaly, whito, and
pearly, near Rudolstadt, agrees essentially with barytea.
314. Baetto-Celebtine, 2SrS + BaS'.
Radiated and foliated. Bluish white. Brittle and friable. H. —
2 -5 ;G. -3-92. Difficultly fusible Lake Erie, Upper Canada, and
Biunenthal.
315. Celestine, SrS!.
Right prismatic ; forms like barytes and anglesite. roo(o) 104*
8' ; P« (if) 76° 58'. Usual combinations fa>,Poo, oo?oo;orthi»
with 00P2 (d) ; also columnar and foliated ; or fibrous, fine
granular, or compact CI. macrodiagonal, perfect ; along Poo less
perfect. H. — 3 to 3 '6 ; G. — 3 9 to 4. Transparent or translucent ;
vitreous or resinous. Colourless, but usually
bluish white to indigo-blue, and rarely reddish
or yellowish. B.B. decrepitates and fuses
easily to a milk-white globule ; colours the
flame carmine-red. Distinguished from barytes
by a splinter, after ignition in the inner flame, pj„ ggg
on being mtJistened with h. acid, and held in
the blue border of the flame of a candle, colouring this of a lively
purple-red. Scarcely affected by acids. C.c. : 43 '6 sulphuric acid
rind 56*4 strontia, but often some baryta or lime. Tantallon
Castle, Calton Hill, Clachnaharry ; near Bristol and Knares-
borough ; sulphur-mines of Girgenti and other parts of Sicily,
Herrengrund in Hungary, Bex, Salzburg, Monte Yiale near Verona,
and M'euJon and Montmartie near Paris. Used for producing a red
light in pyrotechnic mixtures.
316. Anglesite, PbS'.
Right prismatic »f 103° 43'; Pco 75° 35'. The crj-stils, ol
many forms and combinations, are short prismatic, pynunidal,
or tabular. CI. prismatic along o=P, and
basal ; fracture conchoidal ; very brittle.
H. =3; G. -6-2 to 6-35. Transparent or
translucent ; adamantine or" resinous.
Colourless and white, but occasionally yellow,
: ey, brown, or blue ;
Lak white. De-
1 opitates in candle ;
B. B. on charcoal
fuses in the oxygen
flame to a milk-white
bead ; very difficultly
soluble in acids,
wliolly in solution of
tash. C.c: 737
Fig. 395.
Fig. 394.
ead protoxide and 26 3 sulphuric acid. Leadhills (fig. 397), St
Ives in Cornwall, Derbyshire,"
Parya mine in Anglosea,'
ZeUerfeld, Klausthal, Badon-
Fig. 396. Fig. 397.
weiler, Siegen, Silesia, Linares, Phoeniiville in Pennsylvania.
317. Lanahkite, rbS + Pb.
Oblique prismatic. ooP 49° 50*. CL basal, perfect; sectilo; thia
lamina flexible. H.-2 to 25; G. -6 3 to 6 7. Transparent;
Fig. 39a
resinous or adamantine ; on OP pearly. Greenish or ycUowiaS
white, inclining to grey ; streak white, B.B. on charcoal fusea t«
a white globule containing ^jetallic lead; partially soluble in a.
MINERALOGY
401
'acid irith effeireaMncB. C.c: sulphate of lead 67 '6, oxide of lead dyeing, and in manufacturing ink, Prussian blue, and anlphuric
42-4. Leadhills; rare. acid. o . r
HYDROUS SI7LPHATES.
818. UlBXBnJTS{OlauberSaU),'Si^ + loi{,.
Oblijue prismatic, C 72" 15'. CL orthodiagonal ; fracture
CODchoidal. H. — 1 "6 to 2 ; G. — 1 '4 to 1 '6. Pellucid and colour-
less. C.c: 192 soda, 24 8 sulphuric acid, and 56 water. As
an efflorescence in quarries, on old walls, or on the ground ; in
the waters of lakes aud springs in Russia aud Egypt, and on
VesuTias du lara.
319. Gtpsdm, Ca3 + 2fi2.
Oblique prismatic, C 80* 57'. The most common forms are
<»Plll°30'i P138°40'; -P143° 30'; and ooP'oo. Two common
combinations are <»P(/), ooFoo (p), - P (I) {fig. 129), and this
■with P. Lenticular crystals often occur ; heniitropes frequent (figs.
161,150; 151); also granular, compact, fibrous, scaly, orpulverulent.
CI. clinodiagonal perfect, along P much less perfect ; sectile ; thin
plates flexible. H. -1-5 to 2 (lowest on P) ; G. -22 to 2-4.
'Transparent or translucent ; vitreous, on cleavage pearly or silky.
Colourless, and snow-white, but often red, grey, yellow, brown, and
more rarely greenish or bluish. In the closed tube yields water.
U. B. becomes opaque and white ; soluble in 400 to 500 parts of
water, scarcely more so in acids. C.c: 46'6 sulphuiic acid, 326
Jimo, and 20 '9 water.
Transparent crystals, or Sdenite, occur in the salt-mines of Bex
in Switzerland, of the iVrol, Salzburg, and Bohemia, in the sulphur-
mines of Sicily, at Lockpm't in New York, in porphyry at Gourock,
in the clay of Shotover Hill near Oxford, at Chatley near Bath, and
:many other localities. Ftbrous gypsum at Campsie, Matlock in
Derbyshire, and at Ilfeld in the Harz. Compact gj'psum in whole
■beds in many parts of England, Germany, France, and Italy, at
Yolterra in Tuscany (Alabaster) often wiih rock-ilt. The finer
-4ualities-(or alabaster) aoe cut into various oiiiamental articles.
820. KlESEEITE, ligS + fi,.
Rhombic, but chiefly massive. G. — 2"62. Pellucid; greyish
•white. C.c: magnesia 29, sulphuric acid 58, water 13. In beds at
Stassfurt.
821. 'ETSo-axTE {Epsom Salt), iigS + lYi^.
Eight prismatic. P mostly heraihedric ; ooP 90° 38'. ooP (J/),
oofco (o), P (0 (fig. 399). Granular, fibrous, or earthy. CI.
brachydiagonal, perfect. H. -2 to 2 5;
G. = 1 75. Pellucid ; vitreous ; and white.
Taste bitter. C,c: 16-32 magnesia, 32-53
sulphuric acid, and 5115 water. EfSorescence
on various rocks, as at Hurlet near Paisley,
Idria, Montmartre, and Freiberg ; on the
ground in Spain and the Russian steppes ;
in mineral waters, as at Epsom in Surrey,
Saidschitz and Seidlitz in Bohemia. Used in
medicine.
322. GoSLAElTE {White Vitriol), Zn'S
-^7H3.
Right prismatic. ooP 90° 42' ; isomor-
phous with epsomite. ooP, osPot, P (M, o,
I) (fij. 399). Mostly granul.ir or stakctitic ; Fig. 399 (sp. 321).
leniform a-.\d incnistinp;. CI. brachydiagonal, perfect. H. =2to
■*'5; C-. =2 to 2-1. Pellucid ; vitreous. White, inclining to grey,
J«llow, green, or red. Taste nauseous-astringent. C. c : 28 -2 zinc
oiade, 27-9 sulpimric acid, and 43-9 water.
Holywell in Flintshire, Cornwall, Ram-
melsberg near Goslar in the Harz, Falun,
Schomnitz. Used in dyeing and medicine.
323. MoRExosiTE, NiS + 7H,.
Acicular, fibrous, and as an efflorescence.
H. -2 to 2-25; G. -2. Lustre vitreous.
Apple-green; streak white. Soluble. Mor-
vern m Argyllshire, Cape Ortegal (Spain), .
Lake Hurou, Pennsylvania.
824. MELA-\TEniTE {Oran Vitriol, Cop-
ptras), FeS'+7rij.
Oblique prismatic, C 75° 45'. o>P (/)
82* 22' ; - P (P) 101° 34' ; P««o (o) 67° 30'
(fig<400); chiefly jtalactitic, rcniform, or in ^'S- ^O" (sp. 324).
crusts. CI. bx'ial, perfect; prismatic less so. H.-2; G.-1-8 tol-9.
Translucent, rarely transparent; vitreous. Leek- ormountain-greon,
often with a yellowish coating ; streak white. C.c : 26 protoxide of
tion, 29 sulphuric arid, and 46 water. Hurlot near Paisloy,
• ISodcBmais, Kanunelaber;g, Falun, Schemnitz, Bilin. Used in
l(i— 16
325. Smikite, Mn^ + Hj .
Stalactitic aggregates. Rose to white. Felsobanya (Hungary).
826. Mallasdite, liiis'-l-7ftj.
Crystalline foliated masses ; apparently oblique prismatic. Lucky
Bay mine in Utah.
327. Bieberite {Cobalt Vitriol), OoSV7Hj.
Oblique prismatic ; usually stalactitic, or an efflorescence. Pale
rose-red. C.c : 20 cobalt oxide, 4 magnesia, 29 sulphuric acid, and
47 water. Bieber near Hanau, and Leogang.
328. Alunooene (Hair-Salt), AljS + lSftj.
Capillary or acicular, in crusts or reniform masses. H. = 1-5 to
2 ; G. — 1 -6 to 1 -7. Silky. White, inclining to green or yellow.
C.c; 86 sulphuric acid, 16-4 alumina, 48 6 water. Volcanoes of
South America, in coal and lignite in Germany, and on old walls.
329. ALTjmmTE{JVebsteriU), Ai^'+SU.
Reniform, and very fine scaly, or fibrous. Fracture earthy ;
sectile or friable. H. — 1;G. = 17. Opaque ; dull or glimmering ;
snow-white or yellowish white. C. c. : 29 8 alumina, 23 2 sulphuric
acid, and 47 water. Newhaven in Sussex ; Epernay, Auteuil, and
Lunel Vicil in France ; Halle and Mori in Prussia. Felsobanyile,
from Hungary, in rhombic tubes, is similar, but has 10 per
cent, of water.
330. CoQUiMBI-TE, i'ej3S-)-9fl3.
Hexagonal. P 58°. Crystals OP ; with ocP and P ; usually
granular. CI. ooP, imperfect. H. -2 to 2-5; G. -2 to 21.
\Vhite, also brown, yellow,red, and blue. C.c. : 28-6 iron peroxide,
42 6 sulphuric acid, and 28-9 water. Copiapo in Chili, ana Calama
in Bolivia.
3."il. COPIAPITE, 2Fe25S'-fI3Hj.
Six-sided tables, but system uncertain ; also granular. CI. per-
fect. Translucent ; pearly. Yellow. C. c : 34 iron peroxide, 42
sulphuric acid, and 24 water. Copiapo in Chili. Also radiated-
fibrous masses, dirty greenish yellow, incrusting the former,
with 32 sulphuric acid and 37 water. Both probably mixtures.
Fibrofa-rite, also from Chili, and Yellow Iron Ore, from the brown
coa^ at Kolosoruk in Bohemia and Modum in Norway, are both
reniform, or compact and earthy. H. = 2-5 to 3 ; G. -2-7 to 2-9.
Colour ochre-yellow. Apatclile, rcnifcrm-earthy, yeUow, from
Auteuil near Paris, is similar; also Vitriol Ochre from Falun.
Misy, from Rammelsberg in the Harz, containing sulphates of iron,
copper, zinc, and other metals, is a product of decomposiiaon.
332. PissoPHAKE, (Al3F'e.)2S-H5H,.
Stalactitic ; fracture conchoidal ; very ctsily frangible. H. = 2 ;
G. ■=l-9to 2. Transparent or translucent ; vitreous. OUve-green
to liver-brown ; streak greenish white to pa'.e yellow. C.c : 7 to 35
alumina, 10 to 40 iron i>^roxide, 12 sulphuric icid, and 41 water.
Saalfeld and Reichenbach in Saxony.
Carpliosidcrite, reniform, opaque, resinous, and srfraw-yellow, with
a greasy feel, is related. H. - 4 -5 : G. =
2-5. Consists of hydrous sulphate of <j.
iron. Labrador.
333. Cealcakthite, CuS + ofij.
Anorthic ocpw(,i): <»P(x;{r)
19'. P' (P):
120° 50'. P:
o»'P {M) 123' 10' (fi
P' (T) 127°
" 2;'.
40'. P:
Fig. 401 (sp. 333).
water.
Tyrol,
{T):
401). Generally
incrusting. CI.
T pnd M, ira-
perfect. II. —
2-5; G. =2-2.
Blue. C.c: 32
protoxide of
copper, 32 sulphuric acid, 36
Cornwall, Wicklow, Hungary,
Falun, and on lava of YesuviiiA
334. Br.ocHANTiTE, CiiS + sCuH,.
Right prismatic. ooP 104° 32'; Poo
152° 37'; and a>Poo ; also reniform. CI.
brachydiagonal, perfect. H. — 3-5 to 4;
6.-3-76 to 3 9. Transparent or trans-
lucent ; vitreous. Emerald or blackish
green; streak bright green, C.c: 70
Fig. 402 (sp. 334). copper protoxide, 18 sulphuric aclj,
and 12 wtter. _ Sudlodgs (Unst), Roughton Gill in Comber-
XVI. — SI
402
MINEKALOGY
oP (m), ooP'.
knd, Rszbanya, Ekaterinburg ; &lso KrUurig in Iceland
(KrisuvigiU).
335. Lanoite, CuS'+3(iuHj + 2S3.
Eight prismatic. ooP 123° H'. Crystals long-tabular, mostly
in twins. Also in fibro-lamellar and concretionary crusts, witn
earthy surface. CI. basal and brachydiagonal. H. — 2'6; G. — 3'6.
Vitreous. Greenish blue. C.c. ; 66'1 copper protojude, 16'4 sul-
phuric acid, and 18 '5 water. Cornwall.
WarringtomU is similar ; also Konigine from Siberia.
336. JoHANNiTE (Uran-vilriol).
Oblique prismatic, C 86° 40'. ooP 69°. Crystals similar to
trona (No. 291, fig. 383), but minute; airanged in concretionary
and reuiform masses. H. — 2 to2'5 ; G. — 319. Semitransparent ;
vitreous. Soluble. Taste bitter. Bright grass-green. C.c. : oxides
of uranium 6772, oxide of copper 5'99, sulphuric acid 20 '02, water
5*59. Joachimsthal (Bohemia), Johann-Georgenstadt.
337. Blodite {Astrakanite), (MgNa3)S + 2flj.
Oblique prismatic, C 100° 43'. ooP°2 112° 55
(6), <xP-2(»i), <xP°=o (a), -P(p),P«,x>
(d), OP (c) (fig. 403). In prismatic
crystals, or efflorescent. H. =3*5;G.
= 2 '2. Transparent. White or red.
C.c: 47-9 sulphuric acid, 8-5feoda, 12
magnesia, and 21'5 water. Salt lakes
on the Volga near Astrakhan, Ischl,
Stassfurt, and near Mendoza in South
America.
EciissiTie from Seidlitz is similar, but
a mixture.
338. LowEiTE,2(Na2S + MgS) + 5H,.
Pyramidal, but only compact. CI.
basal, distinct; also octahedral, with
angles 110° 44' and 105° 2'. H. -2-5
to 3 ; G. =2-376. Vitreous. Yellow- Fig. 403 (sp. 337).
ish white to flesh-red. Co.: 20 soda, 13 magnesia, 52 sulphui'ic
acid, and 16 water. Ischl.
339. Sykoenite, Ka'S + CaS + Hj.
Oblique prismatic, C 76°. cx>P 73° 65'.
aP««. (b), OP (c), ooP (p), coP<'2 (/'),
ooP°3 (p'"), 2P°2 (e'), P (0'), 2P {o"),
P'cc (jj-P-M (r), P»«, (/), 2P<'» (r"),
-IP"" (e). CI. ojP, perfect; fracture
conchoidal, H. -2-5; G. -2'25. Colour-
less to milk-white. C.c; lime ]6'88,
potash 28 '66, sulphuric acid 48-45,
water 5-47. Soluble in 400 parts of
water. In cavities in halite at Kalusz
(Galicia).
340. POLTHALITE, SCa'S + lilgSVKjg
-^2fi^.
Right prismatic osP 116°. Mostly
fibrous. H.-3-5i G. -2-7 to 28.
Translucent; resinous. Colourless, gene-
rally brick-red. C.c; sulphate of lime
45, of r'"""""'" ""■■= "<■--■•-.•. 1" '-— ^
Bercht
Crystals
Fig. 401 (sp.
;nesia 20-6, of potash 29, 'water 5-6. Ischl, A
339).
ussee,
md
341. Alum, ftS + ^Aljf'caJS'.i-f 24ftj.
Cubic. 0, sometimes with ooOoo and Cm. Generally efflorescent
in fibrous crusts. CI, octnhedrnl ; fracture conclioidal. H. -2to
2-6 ; G.- 1-75 to 1-9. Translucent. White. Taste sweetish-astrin-
gent. Soluble B.B. evolves sulphurous fumes, (a) Polanh Alinn:
KO-KjO; 33-7 sulphuric acid, 10-9 alumina, 99 potash, and 455
water. In the coal formation ot Hurlet and Campsie in Scotland •
the Tertiary brown coals of Hesse and the Khine; the Lias near
Whitby; Silurian alum slates of Scotland, Norway, and Sweden;
the volcanic formations of the Lipari Islands, Sicily, and the Azores.'
(6) Ammonia Alum: RO-(NH,0).j; about \ ])er cent, oxide of
ammonium and 48 water. In closed tube forms a sublimata of sul-
phate of ammonia. Tschermig in Bohemia. (c) Soda Alum-
RO-Na,0; with 7 of soda and 48 water, Mendoza in South
America, Solfatora near Naples, and Milo, {d) Magnesia Alum :
KO-MgO. Translucent and silky. South Africa, Iquinuo in Peru
[PickcringiU), (c) Iron Alum(Pcatlu:r Alum) : RO-FeO. Hurlet
near Paisley, Mbnsfeld in Bavaria, Krisuvig in Iceland. (/) Man-
gancs^Alum: ^.O-HuO. From Dolagoa Bay in South Africa. An
alum with 3'7 oxido of zinc occurs at Folsobanya, and has been
termed Didrichitt.
342. ToLTAITE, SCfo, KJS + 2{J'e3Alj)'S'+12Il3.
Cubic. 0 ; ooOm ; Oa> . Black, brown, or gioen. H. - 3; G. -
Fig. 405 (sp. 343).
Colour ochre-yflilow-
2-79, Solfatara near Naples, Goslar in the Harz, and Kftm-
nitz.
343. Aldsite, 6J3-^3-ij^S-^6H3.
Rhombohedial ; E 89° 10'. Crystals K and OR (fig. 405) ; also
earthy. CI. basal H.- 3 -6 to 4;
G. -26 to 28. Translucent ; vitre-
ous, pearly on 0. Colourless, but
often stained. Hungary, 'Tolfa
(near Civita Vecchia), Lipari
Islands, Auvergne, and Milo.
344. Jarosite, KjS + F'ejSS-l- -
2(Fe.3fIj).
Rhombohedral ; R 88° 58'. CI.
basal ; also fibrous in nodules or
incrusting H. -2-6 to 3-6; G. -3-24.
Spain, Saxony, and Mexico.
345. Gelbeiseneez, 62S + 4Fe2S + 9ftj.
Foliated and massive. H. -25 to 3 ; G, -2-7 to 2-0. Bohemia
Norway, and Tcheleken Island in the Caspian Sea.
346. Ueusite, 'f'e'S-H2}faj3S-t-8H,.
Tcheleken Island in the Caspian.
347. BOTRYOGENE (iJerf VUriol), FejSj •)- 3(F'ej2'S) -I- 3611, .
Oblique prismatic, C 62° 26'. ooP119° 56'. Commonly botry-
oidal. H. -2 to 2-5 ; G, -2. Translucent ; vitreous. Hyacinth-
red and orange-yellow. Falun in Sweden.
348. Herre-nqeundite.
Oblique prismatic, C 88° 50'. Dark emerald-green crystals.
H.-2-5; G.-3-13. C.c: 57-22 oxide of copper, 2304 sulphuric
oxide, 19 '44 water, sometimes with lime. HeiTengi-und (Hungary).
349. Linarite, (PbS + H3Pb)-KCuS + l}jCu).
Oblique prismatic, C 77° 22'. ooP (itf) 61° 41' ; 2P»«. («) 62° 31'.
Crystals c»P°oo (a), OP (c), and the above forms generally. Hemi-
tropes united by ooP°oo (o). CI. orthodiagonal, perfect ; fracture
36° 10'.
Fig. 403.
conchoidal. H. *= 2 -5 to 3 ; G. = 6 -2 to 5 -45. Translucent ; adamant-
ine. Azure- blue to dark blue; streak pale blue. C.c: oxide of
lead 56-69, oxide of copper 19-83, sulphuric acid 19*98, water 4-5.
Leadhills, Red Gill and Roughton Gul (Cumberland), Linares in
Spain, and Nertchinsk.
350. Caledo.s-ite, 5PbS-H2(H3f'b)-l-3(H30u)-
Right prismatic ooP (m) 95°; Poo (c) 70° 57'; 2Pa
Crystals frequently as in fig, 407, but gene-
rally hemihedral, CI. brachydiagonal, a dis-
tinct; m, cimperfect, H, -2-5 to 8 ; G. - 64.
Transporent ; resinous. Verdigris-green and
mountain-green ; streak greenish white. C,c:
68-42 oxide of lead, 1017 oxide of copper,
17-3 sulphuric acid, 4-05 water. Leadhills, ;
Red Gill in Cumberland, Rezbanya in Tran-
sylvania.
351. LETTSO.MITE, SCujS ■^ 2(Als3H3) -H
1511^.
Right prismatic; but in tufts of capillary
crystals with velvet-like appearance. Colour r.- ja-j / ocrt\
smalt-blue to sky-blue, dc: 49 oxide of ^.g, 407 (sp, 350).
copper, 2-97 lime, 11-21 alumina, 141 oxide of iron, 121 sulphuric
acid, 22 5 water. ^loldaw-a in the Banat. lyoodwardiU is,
probably an aluminous variety
of the above. Turquoise-blue
to greenish blue. Coinwal).
352. Kainite, JJgS + KCl
■fSrt..
Oblique prismatic, C 85° 5'
(iig408). G, -2-13. CLortho-
diogonal. White to reddish.
C.c : 18-1 magne.-iia, 15-7 potash, 32-2 sulphuric acid, 14'S chlorine,
21 -7 water. SUssfui t.
Fig. 408 (sp. 352).
MINERALOGY
403
Fig. 409 (sp. 355).
TELLURATES AOT) CHROMATES.
85S. VotnAKiTB, '6^'i'e + 262 .
locrutiDg, euthy. Lustre waxy. YeUovish. Opaqne. O.c.
bismuth 66 S, teUorium 26-8, water 5 '9. Highland in Montana.
S64. MiONOtiTE, flgf e .
'White acicular crystals from Keystone mine in Colorado.
866. Cbocoisite, tbCir.
Obliqne prismatic, C 77° 27'. odP 93° iH (M), - P 119° 12' «)
eoP^m SS" 10', <»P«oo {g\ (fig. 409).
CI. ooP, distinct; soctile. H. -2-5 to
t ; G. - 6 -9 to 6 1. Translucent ; ada-
mantine. Hyacinth- or aurora-red ;
strvak oniDge-yeUow. G c. : 31 chromic
ncid, and 69 lead protoxide. BerezofT,
Mnrsinsk, and Nijni-Tagilsk in the
Urals, Congonhas do Campo in Brazil,
Rezbanya, Moldawa, and Tamowitz.
Used as a pigment, but not permanent.
356. PH0BNico-CHEOlTi;,2f'bCr+l'b.
Right prismatic ; dimensions un-
known. H. -3 to 3-6; 0.-575.
Translucent on the edges ; resinous
or adamantine. Cochineal- to hya-
cinth-red; streak brick-red. Co.: 23 chromic acid! and 77 prot-
oxide of lead. Berezoff.
367. Vacqueunite, 2(2f'b■er+f'b)-^(2CuiJ■r-K^l).
Oblioue prismatic, C 67° 16'. Crystals OP, -P, -P<>oo for P
f, h), always twinned (Bg. 410), the faces of OP
forming an angle of 134' 30'; also botryoidal or <I
reniform. H. = 2-5 to 3 ; G. - 5 5 to 5 8. Semi- '•'*
translucent or opaque; resinous. Blackish or -j^ „„
ilark oUre-green; streak siskin green. C.c: 61 ^'g- 410.
lead protoxide, 11 copper protoxide, 28 chromic acid. Leadhills
Berezoff, Congonhas do Campo (Brazil).
MOLYBDATES AND TUNGSTATES.
868. ■WuLTByiTE, fbilo .
4i&):"'k^pfCta'e;''''«'"'*^^'^'^-"^('^'-«^2W(«8«-
fiacture uneven, or con-
clioidal. H. -3; G. =6'3
to 6 '9. Pellucid; resinous
to adamantine. Orange-
yoUow, honey-yellow and
colourless. C.c: protoxide
of lead 61 5, molyodic acid
33 '6; red varieties have
some chromic acid. Lack-
entyre in Kirkcudbright
(fig. 412), Bleiberg, Rez-
biinya, Pennsylvania, Za-
catecas. ZPbOMoO, +
CaOUoO,, with 6-88 of
lime, occurs in Chili.
Fig. 414 (sp. 358).
Fig. 413 (sp. 358).
869. EosiTE.
Pyramidal. OP (c) :p'H7'10' ; p* :p 125°40'(fig. 415). H.-S
to 4. Colour deep aurora-red. Streak orange-
ycUow. Avanadio-molybdateoflead. Lead-
hills.
360. Meoabasite, Mg^W, .
Oblique prismatic; similar to wolframite.
Ill fine needles. H. -3-5 to 4 ; G.-6-45 to
6 97. Vitreous to adamantine. Yellowish
brown to brownish red, translucent hyacinth-
red j streak ochre-yellow. C.c: protoxide
of manganese 231, protoxide of iron 6-4,
tungstic acid 71 5. Schlaggenwald, Sadis
dorf, Morococha in Peru.
361. SCHEELITE, CaW.
i,?/!^*'"^?,',' "i"' ™"°y "f *''« modifying planes hemihedric P.
n3'S2'. CL 2P.0 (n) 130° 83', perfect; TPand OP less so. Frac-
ture concho.dal. H. -4 to 4-5 ; G. -5-9 to 6-2. Translucent ;
resmona to adamantine. Colourless, and grey, yellow, or brown ;
reak white. C.c: 19 -4 lime, 80-6 tungstic acid. Caldbeckfell near
Fig. 416 (sp. 359).
Keswick, Pengelly in Cornwall, Zinuwild. Schlaatenwald. Salz-
burg, Chili, Si- - -
Fig. 416 (sp. 361,.
Pyramidal, generally hemihedric P.
131 25', Crystals sometimes spindle-
shaped. CI. P, imperfect H. ■=3;G.-
7■9to8•l. Translucent ; resinous. Grey,
yellow, brown. C.c: 48-4 protoxide of
lead, 61 '6 tungstic acid. Keswick, Zinn-
wald, Coquimbo (Brazil).
363. Reinite, JeW . Fig. 417 (sp. 351).
Pyramidal. P 103° 32f^ basal angle 122° 8'. CL ooP. H.=4;
G. — 6'64. C.c: protoxide of iron 234, tungstic acid 76-45.'
Eimbosan in Japan.
864. Wolframite, (S-e, An) Vt.
Obliqne prismatic, C 89° 22'. ooP tU] 100° 37', - *P<>oo (P'l
:' 54'. Pem I,l\ OS" a' - '> • ■ ■ ■-• " - ^ '
»P»2 (6),
Kg. 418.
61° 54', P«co («)' 98° 6', a.P<o (r),
i2P«2(s). Twins common. Also lamjnar.
CL cUnodiagonal, perfect; fracture un-
even. H.-5 to 6-5; G.-71 to 7-5.
Opaque; resinous, metallic, adamantine
on the cleiva^. Brownish black ;
streak black (varieties with most iron) to
reddish brown (most manganese). C. c. :
76 tungstic acid, 9-5 to 20 protoxide of
iron, and 4 to 15 protoxide of manganese,
in some with I'l niobic acid. East
Pool, Cambrae, and mines near Redruth;
Godolphin's Ball in Cumberland ; Alten-
berg, Gcyer, Ehrenfriedersdorf, Schlag-
genwald, Zinnwald, the Harz ; also
Urals, Ceylon, and North America.
FerbcrUe, with 26 protoxide of iron
and2^eW-fl?e(a-*to-4-6; 6.-67 to 6-8), from Spain, may ba
different.
365. HiJBNERiTB, MnW.
Eight prismatic ooP (if), if: if 105°. 01. o.?oo , perfect ■
usually foliated or columnar. H. -4-5; G. -7-14. Adamantineon
cleavage ; elsewhere greasy. Brown-red ; streak yellow-brown.
C.c : protoxide of manganese 23-4, tungstic acid 76 6. Mammoth
district in Nevada,
ANHYDROUS PHOSPHATES, ARSBNIATES, AND
TANADIATES.
366. Xekotime, "i^P.
PyramidaL P 82° 22' middle angle; pokr anele 124° 30'
Crystals P; »? ; ooPoo. CL loP.
H. -=4-6; G. -4-6 to 4-55. Translucent
in thin splinters ; resinoos. Yellowish
and flesh-red. C.c: 62 yttria, and 88
phosphoric acid ; but some with 8 to H
cerium protoxide. Lindesnaes and Hit-
tero in Norway, Ytterby (Sweden),
Georgia, and ( Wiseriiu) St Gotthaii
367. Crtptolitr, Cej^'j.
Acicular crystals, embedded in apatita
G. = 4-6. Transparent. Pale wine-yellow. Powder soL in con-
s. acid. Wbhler found 7370 cerium protoxide, 27-37 phosphoric
acid, and 1-51 iron protoxide. Occurs in
the apatites of granite in Scotland, biSt not
in those of limestones. Also at ArendaL
368. MoNAziTE, (Ce, La, 'fh),?,.
Oblique prismatic, C 76° 14'. ooP 93°
23' ; crystals (fig. 420) generally thick or
tabular. CI. basal, perfect; translucent on
edges. Flesh-red and reddish brown. C.c:
28 phosphoric acid, 87 to 46 cerium prot-
oxide, 24 to 27 lanthanum oxide; that from
Zlatoust from 18 to 32-5 of thoria. Notero
in Norway, Miask, Norwich in Connecticut, and the Rio Chico ia
Colombia. Tuneritc, from Dauphin^ in complex transparent
honey-yellow crystals, ia manazit«,
Kg. 419 (sp. 366).
Kg. 420 (sp. 368).
404
MINERALOGY
369. TRiPiiTLITE^(2I'c + Lij)P,.
Kight [irismatic. ooP 133°; chiefly granular. H.— 6; O.— 3'6.
Ko!<inous. Greenish grey with blue spots. Co.: iron protoxide 40,
ni.iui^auese protoxide 6*6, littna7'5, itliosphoric acid 45. Boden-
iiiui» in Havuria. Nom'ich in Massachusetts. LilhiophiliU^ from
Fairfield (Connecticut), is a mnngancsian triphylite.
370. BFKZE1.I1TE (fuAni'te), (CaligjjAa, .
MiLssivo. H. -5 to 6; G. -2-62. Co.: lime 23, magnesia 15,
arsenic acid 60. Sol. in n. acid. LAngban (Sweden).
371. Arseniatf. OF Nickel, KijAa,.
Amorphous. H. -4", G. — 4 98. Sulphur-yellow. C.c: oxide of
nickel 48*2, arsenic acid 50'5. Johann-Georgenstadt.
372. NiOKKLEIU!, lfij'A's3 + 21^i.
Crystalline massive. G. — 484. Dark grass-green ; streak lighter.
Co.: oxide of nickel 021, arsenic acid 36 6. /ohann-Georgenstadt.
373. Dechenite, (rb2;n)V,.
Botryoidal and stahctitic. H. -3 to 4; G-5-8'2. Lustre
resinous to greasy. Yellowish red, deep red ; streak orange to pale
yellow. C.C.: 677 oxide of lead, 15 8 oxide of zinc, 24 2 of vanadic
acid. Wanlockhcad, Freiburg (in Baden), Lauter Valley.
374. PsiTTACiNiTE, 3(l''b,V,) + <5ujVj -H eCnii, .
Manimillated and incrusting. Siskiu- to olive-green. C.c:
vanadic acid 19'3, le.id oxide 53'2, copper oxide 18'95, water 868.
Silver Star (Montana).
375. Pucherite, 'Bi,V..
Right prismatic ooI'i23°55'. H. - 4; G.-6-25. 01. basal, per-
fect; vitreous. Kod or reddish brown; streak yellow. Easily soluble
inacids. C.c: bismuth oxide71'7, vanadic acid 2S'3. Scbneeberg.
376. Atopite, Ca..Sb , .
Cubic (figs. 30 witli 26 and 33). H. -5-5 to 6; 0.-6. Lustre
greasy; yellow to resln-browo. Translucent C.c: antiinonic acid
73 2, lime 17'5, iron protoxide 2'7, magnesia 15, soda 4 3. L&ng-
ban (Wermlaud).
HYDROUS PHOSPHATES, io.
377. Brusiiite, {SCa-nftj)3'P'.-Hft,.
Oblique prismatic, C 62° 46'. Needle crystals. H. -2 to 2-5;
C.-2'21. Vitreous. Co.: liroc 320, phosphoricacid 41'3, water
tu'i, Aves Islands and Sombreio (Antilles).
378. Newdertite, MgjH., '\\ -f 6flj .
Hightprismatic. CI. brachydiagonal. C.c: phosphoric acid 41 '25,
magnesia 23, water 357. From guano, Skipton Caves, Victoria,
379. Haidingerite. Ca^As, -h 3H, .
Eight prismatic mP 100*. CI. perfect j sectile, flexible.
H. -2 to 2 5 ; G. -2-8 to 29. Otherwise like pharmacolite (sp.
BSl). C.c. : 85-68arscniateoflimc,andl4'32 water. JoachimsthaL
3S0. RosELrrE, SjAsj-f 2Hj.
Anorthic. CL macrodiagonal. Rose-red ; streak white. H. —
35; G. -3-46. C.c: 25 5 lime, 103 cobalt oxide, 3'6 magnesia,
62 i arsenic acid, 8'2 water. Schncoberg.
331. Pharmacolite, 2CaA's.-f cH..
Oblique prismatic, C 65° 4' (fig. 421). ooP (/) 117° 24', - P (J)
139° 1?', -»P (n) 141° 8', tPOo) (o)
83° 14', ooP-S (?) 167° 6'. Crystals
generally acicular and radiated. CI.
cUnodingcnal, perfect ; sectile and
flexible. H.-2 to 2-6; G.-2-6 to
28. 'Translucent; vitreous. Pearly
white. Yields water in the closed
tube. C.c: arsenic acid 51, lime 25,
water 24. Audreasberg. Biebsr, Mnr-
kircben, Wtticben. Generally mixed with orythrite
382. ■Wapflerite, 2daAs-f Sfl,.
Anorthic; coP' (m), ooT (.1/), o.P'2
(«), a.'P.2(i^, .I'oo (d), 'P,» (D),
3,f'a> ((), S'?,* (T), 2r'2 (p), 3f'4 (y),
3'1'} (<7), 4?4 («), 2,^2 (-). oof-* (h)
(fig. 422); also incrusting and globular.
01. clinodiagonnl. H. - 2 to 2-5 ; O. -
2 48. Colourleas. Vitreous. C.c:
lime 15 6, magnesia 7 '4, arsenic acid
47 6, waUr 89-5. .loaohimsthal.
383. HoRKMiTB, MgjAs-t-SH,. Kig. 422 (sp. 3S2).
Oblique prismatic. o.P lO/*. H.
-5tol- 5 -2-47. Vhito. Trau«luc«nt ; pearly. C.c: 24-3
magnesia'. 2914 water, 46 56 arsenic acid. ProUhlylromHungmrr.
d'^fy'
.V
i
ir
\ **
T
\
r
l^y^
. 423.
(T).rco (J/) J
384. Vn-IAh-iTE, 3Felf',-^8li,.
Oblique prismatic, 0 75° 34'. JbP (in) 108° 2' ; P (f) 120* 26*,
P°oo(k!) 64° 40'. CrysUls prismatic (figs. 423, 4241 ; also fibrons
or earthy. CL clino-
diagonal, perfect ; thin
laminaj flexible. H. -2;
G. -2-6 to '27. Trans-
lucent or transparent ;
vitreous, or bright pearly
on cleavage. Indigo-
blue to bl.ickish green ;
streak bluish white, but
soon becomes blue on
exposure. C.c: S3"l
iron protoxide, 12"2 iron
peroxide, 29 phospho
acid, and 2"
Transparent
coloured crystals at St
Agnes in Cornwall, and
AUentown and Inileytown in New Jersey ; earthy in Cornwall,
Styria, North America, Greenland, and New Zealand ; and in peat
mosses in northern Germany, Sweden, Norway, and Shetland.
3S5 Svmplesite, te^Ks^ + SU,.
Oblique prismatic ; in minute acicular crystals. CL ditto-
diagonal. H.— 2"5; G. — 2"96. Vitreous. Cleavage face pearly.
Celadon-green to pale indigo ; streak bluish white. Lobenstciu
in Reuss, and Lolling in Carinthia.
386. Erythrite, CojAsj-l-8Hj.
Oblique prismatic, C 55° 9'. ooP'^oo (P), ooP",
also ooP3 (t), and P (/) 118° 23' (fig. 425).
CL clinodiagonal [P), perfect ; sectile ; thin
lominn: flexible H. - 1 5 to 25; 0.-29
to 3. Translucent ; vitreous, pearly on the
cleavage. Crimson or peachblo-ssom-red. C.c;
38-2 arsenic acid, 37-8 cobalt protoxide, 2-1
water, but often with nickel 9. CornwnlL
Alston in Cumbcrlond, Alva in Stirlingshiie.
Schneeberg, Saalleld, Allemont, Rieclielsdorf,
the Pyrenees, and lloduni in Norway.
KcMtUschlag or Earthy Incrusting Cobalt,
rcniform, is a mixture of er\-lhrine with arseni-
ous acid. Lairtidulan, thin rcniform lavender-
blue crusts, translucent, resinous, or, vitreous
(H. -25 to 3; 0.-295 to 3 1), consisting of
arsenic acid, protoxides of cobalt, nickel, and copper,
from Annaberg.
387. KoTTioiTE, {in, Co, l}i),A"sj-f8ll.
Oblique prismatic ; massive or in crusts, with crystalline surface
and fibrous structure. 01. clinodiagonal, perfect H. — 2'5 to 3;
G. -3 1. Lustre of fracture silky. Colour light carmine and pcach-
blossom-rod, of different shades ; streak reddish white. Translucent
to subtransluccnt C.c: 30 52 tine oxide, 6 91 cobalt oxide, 3
nickel oxide, with arsenic acid. Schneeberg.
388. Annabergite (.Vid«I Ockre), Sij.is -I- 8H, .
Oblique prismatic ; in capillary crystals, also earthy ; sectile
H. -2 to 2-5 ; G -3 to 31. Dull or glistening. Api>le-grecu or
greenish white; streak greenish white and shining. C.c; 387
arsenic acid, 37 3 nickel protoxide, and 24 water, but with a littlo
cobalt or iron. LcadhiUs, Pibble in Kirkcndbriglit, Audreasberg,
Saalfold, Riechelsdorf.
SS9. LuDLAMiTE, Pe72P, + 9H,.
Oblique prismatic, C 79° 27'.
(fig. 426). 01. OP, perfect
H. -3-5; G. -312. C.c:
53 06 oxide of iron, 29 83
phosphoric acid, 17'0 water.
ComwalL
S90. FiLLOWITE, S(ft,^,) + H3
Oblique prismatic, C 89° 51';
pscudo-rhombohedral. P;-2P8;0P. 01. basal. H.-4-5;C.
-343. Resinous to greasy. W.ix-veUow to red-brown, oi
colourless; streak white; translucent fc.c: phosphoric acid 40-2,
iron protoxide 6'S. manganese protoxide 40*2, lime 5"2, soda 58,
water 17. Branchville (Connecticut).
391. HcREACiiTE, 5(Mn, fe)2P,-l-5rt5.
Oblique prismatic, 0 S9° 27'. ooP 61°. Fracture conchoidaL
E.-3-5; G. -5 2. Translucent; resinous. Reddish yellower
brown. B. B. fuses easily to a black metallic globule. Soluble in
acids. C.c : 39 phosphoric acid, 8 iron protoxide, 12 manganese
protoxide, and 12 water. Hurcaux near Limoges.
oP 131° 23': OP; P 111° 29'
Fig. 426 (sp. SS9).
MINERALOGY
405
BeUmiU. H. — 5; G. -3'5. Opaqoe ; Titreous or resinons.
Dark Tiolet or blae to greenish erey ; streak violet-blue or crim-
son-red. Contains more iron anil less manganese than the above.
Hnreanz.
392. DiCKi.vsONITE, 4(ft,Pi)-H3fir,. .
Obliqne prismatie, C 60° 30'. Crystals tabular. CI. basal, per-
fect H. -3'5 to 4; G. -3 34. Vitreous; pearly on cleavage.
Olive- to oil-green, and grass-green; streak white. Transparent;
brittle. Co.: phosphoric acid 40, iron protoxide 12'7, manganese
protoxide 25, Ume 11-8, soda 6-6, water 3 '8. Branchville (Con-
necticnt).
393. TaiPLorDiiTE, (Jln, Fe)^P,+fij(Ai, te),.
Oblique prismatic, C SI' 56'. Generally fibrous ; transparent ;
resinous to adamantine. H. — 4 6 to 5 ; G. — 3 7. Yellowish-brown.
C.C.: 4845 oxide of manganese, 1488 protoxide of iron, 321 phos-
phoric acid, 4 1 water. Fairfield (Connecticut).
S91. FilaPtELDtTE, kyV,+ 2tl,.
Anorthic; usually foliaceous. H.-3'5; G. -3-15. WTiit* to
straw-yellow ; streak white. Pearly to brilliant-adamantine on
cleavage. Transparent ; brittle. C.c: phosphoric acid 38 4, iron
protoxide 56, manganese protoxide 15 "6, lime 30, soda 7, water
:0. Fairfield (Connecticut).
395. Chondrabsen'ite, MnjAJs^ + lfij.
In small grains. H. =S. Yellow to reddish-yellow. Trans-
lucent ; brittle ; fracture conchoidaL Faisberg mines (Werm-
land).
H96. Reddisoite, &n^,,+SU,.
Right prismatic. P ; P2 ; o»?oo. H. -3 to 35; G. =31.
Vitreous; rose-pink to yellowish white. Translucent; fracture
uneven; brittle. C.c. : phosphoric acid S4'£, iron protoxide 5 •43,
manganese protoxide 46 '3, lime '8, water 13 1. Branchville.
397. SCOEODITE, Fe,As.j + 4Hj.
Right prismatic P with polar edges 102° 52" and 114° 40*.
Crystals P (p), ooPoo (o), and ooPoo (6) ; also OP, 4P (i), ooP («),
2P2 (j), ooP2 (<0 120° 10', and iVon (m)
132' (fig. 4*27); also columnar and fibrous.
CI. imperfect; brittJo. H. -35 to 4;
G. =31to3'2. Translucent: vitreous.
Leek -green to greenish black, also indigo-
blue, red, and brown. B.B. fuses easily,
with arsenical odour, to a grey magnetic
slag. Sol. in h. acid, to a brown solution.
C.c. : 498 arsenic acid, 34 6 iron peroxide,
and 15 6 water. St AustcU in Comw.ill,
near Limoges in France, Schwarzenberg,
Lolling in Carintliia, Brazil, and Siberia.
398. Stresgite, 'Fe.P,-i-4H2.
Right prismatic. P with polar edges
101° 38' and
115° 36', mid-
dle edge 111°
30'. ooP2 (rf)
and 00 Poo (r),
P (P), OP (A),
2r'oo (m) 48°
(fig. 42$). Cry-
stals go iiei-ally
r, P,d; r do-
minant CL r. H. - 3 to 4 ; G. -2-87.
Cherry-red. Translucent C.c. : prot-
oxide of iron 4318, phosphoric acid
37-42, water 19 4. Rock Bridge (Vir-
ginia). Fig. 428 (sp. 398).
399. DtrTREHiTE (KrauriU), 2FejP, + 3fl,.
Right prismatic ooP about 123'. Spherical or reniform. CL
brachydiagonal ; brittle. H. =3 to 3 5 ; G. =3-3 to 3-4. Trans-
lucent on the edges, or opaque ; shining or dull. Dirty Icek-green
or blackish green; streak siskin-green. C.c : 63 iron peroxide,
28 phosphoric acid, and 9 water. WesterwalJ, Hirschberg, and
Limoges
400 ■Berjutvite, 5Fej3pj + 14Hj.
<«cur8 in small foliated and columnar aggregates. CI. plane
metallic pearly. H. -2 ; G. -2878. Colour hyacinth-red to
reddish brown ; streak dirty-yellow. C.c : 54-5 peroxide of iron,
■-'8 -65 phosphoric acid, and 16 55 water. Bohemia, Scheibenberg
in 84xonj.
Fig. 427 (sp. 397).
401. Eleonoeite, 3'Fe^■p,■^8fi,.
Oblique prismatic, C 48° 33'. Twin face the orthopinacoid.'
CT. a.P°oo. H. -3 to 4. Dark hyacinth-red ; streak yellow.
Vitreous to pearly. C.c : 5194 peroxide of iron, 31 '88 phosphoric
acid, 16 '37 water. Eleonore mine near Bieber.
402. Cacoxeke, 2Fe,Pj-i-12H,.
Radiated tufts, of a brownish-yellow colour. H. — 3 to 4 ;
G. - 3 -38. Sol. in h. acid. From the Hrbeck mine near Zbirow in
Bohemia.
403. Phabmacosidebite {Ouie Ore), 4fej3AJ9,-H6lij.
Cubic and tetrahedral ; osnally ooOoo , with ^, or ooO. Brittle.
H. ■=2-5; G. -2-9 to 3. CL oiOoo. Semitransparent to translu-
cent ; adamantine or reainona. Olive- to emerald-green, honey-
yellow, and brown ; streak straw-yellow. Pyro-electric C.c: 43
arsenic acid, 40 iron peroxide, and 17 water. Carharrack in Corn-
wall, Burdle Gill in Cumberland, Lobenstein in Reuss, Schwarzen-
berg in Saxony, North America, and the gold quartz of Australia.
404. Calaite {Turquoise), 2(mJP, + 5H,.
Massive, reniform, or stalixctitic ; fracture conchoidal. H. = 6 ;
G. — 2 6 to 2 8. Opaque or translucent on the edges ; duU or vzxy.
Sky-blue, greenish blue, rarely green ; streak greenish white.
C.c : 47 alumina, 32'5 phosphoric acid, and 20'5 water, but mixed
with phosphate of iron and copper. Silesia, Lu^atia, and ReusSL
Oriental turquoise, in veins, at Meshed, near Herat ; in pebbles in
Khoras.-in, Bokhara, and Syrian desert Takes a fine polish, and
is valued as an ornamental stone, but is destroyed by oil, and
deteriorated by soap.
405. VrATELUTE(iaitontfe),3Alj2i'3 + 12H,.
Right prismatic ooP 126° 25 ; Foo 106° 46'. Crystals ooP»
(P), ooP (d), Poo (o) (fig. 429) ; but generally small, acicnlar, and
in radiated-hemispherical and stellate-fibrous masses. CL alon;;
ooP and Poo , perfect H. - 3 5 to 4 ; G. - 2 -3 to 2 5. Translucent ;
Titreous. Colourless, but generally yellowish or greyish, . j.
sometimes green or blue. C c. : 38 alumina, 35 '3 phos- Kj^qX
phoric acid, and 267 water; but generally traces of I [. I I
jluoric acid (2 per cent). Shiant Islands and Glencoe li I I
in Scotland, Barnstaple, St Austell, near Clonroel and \_HJ
Portrush, Beraun in Bohemia, Amberg in Bavaria ; also
in New Hampshire and Tennessee. C'<rrula>lactin, from ''8- *~-
Nassau, has two equivalents less of water.
406. Variscite, 'a1jPj-h4H,.
Right prismatic ; reniform ; conchoidal fracture. H. = 4 to 5 ;
G. ="234 to 238. Apple- and emerald-greenj streak white. C.c:
32'4 alumina, 44*85 phosphoric acid, 2274 water. Messbach in
Reuss, Montgomery county in Arkansas.
ZepharomchiU from Bohemia contains one equivalent more water j
Era-iuiU from Hungary two equivalents more.
407. FiSCHEElTE, 2'AljJ'j-H8lij. ,
Right prismatic ooP 118* 32'; generally in crystalline crusts.
H. = 5; G. — 2*46- Grass- and olive-green. Vitreous lustre. C.c:
alumina 42, phosphoric acid 29, water 29. Nijni-Tagilsk.
408. Peca-Vite, 2Ai,Pj-H6H2.
Right prismatic ooP 127°. In thin reniform crusts, of fibrous
structure. H. -3to4; G. -249 to 254. Grass- and emerald-
green. Vitreous or greasy lustre. C.c : alumina 45, phosphoric
acid 31 3, water 23 7. Striegis in Saxony.
409. HoPEITE, Znji» + 4Hj.
Right prismatic oop2 82° 20'; P with polar edges 106° 36' and
140°. CL macrodiagonal, perfect H. = 25 to 3 ; G. = 276 to 285.
Vitreous or pearly. Greyish white. C.c: oxide of zinc 35'21,
phosphoric acid 31*1, water 15'8. Altcnberg.
410. Adamite, 4ZnAs,-fHj.
Right prismatic ooP 91° 52'. CL macrodomic H. =3-5;
G. = 4 *34. Lustre vitreous. Colonr honey-
yellow to' violet ; streak white. Trans-
parent C.c: oxide of zinc 56 '6, arsenic
acid 40 2, water 3 2. Cape Garonne
France, Chanarcillo in Chili
411. LlBEfHESITE 4CuPj-H6H3.
Right prismatic. o.P (u) 92° 20', f «
(o) 109° 52', and P (fig. 430). H.-4;
G.- 3 6 to 3 8. Translucent on the edges;
resinous. Leek, olive-, or blackish-green;
streak olive-green. C.c. : 66 copper prot-
oxide, 30 phosphoric acid, and 4 water. ''i- *'" (»P- *"'•
GonnisUke (Devon), Libethen (Hungary), Nijni-Tagilsk.
406
M I N.E B A L 0 a.Y
412. OLrvENiTE, 46a (A'sj^'j + ll,.
Right prismatic. »(P) (r) 92° SV, f<o (/) 110' 60', oopoo (n)
(fig. 431); also spherical and reniform, and
columnar or fibroofl, CL (r) and (Z), im-
perfect. H. -3; G. -4-1 to 4-6. Pellncid
ia all de^eea ; vitreous, resinous, or silky.
Leek-, olive-, or blackish-green, also yellow
or brown ; streak olive-green or brown.
B.B. in the forceps fuses easily to a dark
brown adamantine bead, covered with
radiating crystals ; on charcoal detonates,
emits arsenical vapours, and is reduced. [ j
Sol. in acids and ammonia. C.c. : 56 "S
copper protoxide, 30 '6 crsenic acid, and 4
water ; but alsp 1 to 6 phosphoric acid.
Carh^rack, Tin Croft, Gwennap, and St
Day in Cornwall ; Alston Moor, Thuringia, pj^ 431
Tyrol, Siberia, ChilL
413. Veszeltite, SOu, ei.n, %, A'sj + lSftj.
Obliquo prismatic, C 103° 60'. H. - 3 -6 to 4 ; G. - S-63. Green-
ish blue. C.c. : copper 37-34, 25-20 zinc oxide, 10-41 arsenic acid,
9-01 phosphoric aoi<t 17'05 water. Moravicza (Banat).
414. Desoloizite, iPbY^+H,.
Right prismatic. ooP 116° 26'. H. -S'S ; G. -5-88 to 61.
Olive-brown to blaok. C.c. : 56-48 oxide of lead, 16-6 oxide of zinc,
1-16 oxide of manganese, 2274 vanadic acid. Sierra de Cordoba
ia the Argentine Republic.
415. VOLBOBTHITE, 4{(5u, Ccl) Vj + Hj.
Hexagonal ; small tabular crystals, OP , <»P, single or in groups.
Generally massive. H. -3; G. -3-45 to 3 -89. Olive-green;
streak almost yellow. B.B. on charcoal fuses easily and forms a
graphite-like slag, containing grains of copper. Sol. in n. acid, and
with water gives a brick-red precipitate. C.c. : 37 to 38 vanadic
acid, 39-4 to 46 copper oxide, 18-5 to 13 lime, 3-6 to 5 water.
Sissersk (Urals), Nyni-Tagilsk, and Friedrichroda in Thuringia.
416. Tagilite, 4Cufj + 3H,.
Oblique prismatic ; but botryoidal and radiating-fibrous, or
earthy. H."-3;G. — 4. Emerald-green. C.c. : 618 copper prot-
oxide, 27 7 phosphoric acid, and 10-5 water. , Nijni-TagUsk, and
near Hirschberg.
417. EOOHROITE, 4Cu'A3J■^7fl,.
Right prismatic. ooP (M) 117° 20', t«)()i) 80° 62', with ool>2
(/) and OP (P) (fig. 432). Brittle. H. =3-5
to 4 ; G. = 3 -35 to 3 45. Translucent ; vitre-
ous. Emerald- or leek -green ; streak vor-
digris-gi'een. B.B. in forceps fuses to a
greenish brown crystallized mass. Easily
sul. in n. acid. C.c. : 47 copper protoxide,
34 arsenic acid, and 19 water. Libetheo in
H ungary.
418. Erinite, 5Cuia, + 2ft3.
Reniformandfoliated; conchoidal fracture. .,_,
H. -4-5 to 5; G.=4t<;4-1. Translucent on Fi«. 432 (sp. 417).
the edges; dull resinous. Emerald- or grass-green ; streak similar.
C.c: 59-9 copper protoxide, 34-7 arsenic acid, and 6-4 water.
Cornwall. ComvKtllitc has 3 or 6 of water.
419. DlHTRITE, 6(JuV'., + 2H,.
G. - 4-4. Oxide of copper 69, phosphoric acid 24-7, water 6 -25.
Rheinbreitenbach and Nijni-Tagilsk.
420. MOTTEAMI-FB, bifia, tb)V'j + 2Hj.
Black crystalline crusts; streak yellow. H. — S; 0. — 5-9.
C.c, : oxide of copper 20 4, oxide of lead 7-2, vanadic acid 18-7,
.water 3-7. llottram in Cheshire.
421. EHLiTE5(iu'Pj + 3fij.
Right prismatic ; botryoidal, radiating, foliated. H. — 1 "6 to 2 ;
G. = 3 -8 to 4 -27. Translucent on the edges ; pearly on the cleavage.
A'erdigris-green ; streak paler. C.c. : 67 copper protoxide, 24
phosphoric acid, and 9 water. Ehl on the Rhine, Nijni-Tagilsk,
Libethou.
422. Tybolite, 6Cu'A'8j + 9Hj.
Right prismatic. CI. basal, perfect ; reniform. Radiate-folia-
ceous. H. -1-5 to2; G. -3. Lustre pearly on cleavage face. Colour
ai»ple-green and verdigris-green to sky-blue ; streak paler. Sub-
translucent. C.c. : oxide of copper 60S, arsenic acid 292, water
20-5. Tyrol, Hesse, Thuringia.
423. PnospnoROoaALCiTE (i«nntfe), eCuK"^ -f Sfl, .
Obllaui-. prismaUc. CrystaU mP** (/} 38° 6«', P [P) 117' «',
with OP (o) and ooP'oo («) (fig, 433) ; usually gmall and indistinct;
more common in spherical or renifoi-m and
radiated-fibrouB masses. H. — 6; G. =>4-l
to 4-3. Translucent throughout or on the
edges; adamantine to resinous. Blackish-,
emerald-, or verdigris-green. C.c. : 70-8
copper protoxide, 21-2 phosphoric acid,
and 8 water. Cornwall, Rneinbreitenbacb,
Nijni-Tagilsk.
424. Clinoclase, 6(iuXa3-)-3H,.
Oblique prismatic, C 80° 30'. OP (F),
ooP(m) 66°, JPoco (a) 99° 30', (r) 123° 48'
(figs. 434, 435) ; and hemisphericaL CI.
basal, perfect. H. -2-5to3; 0.-42 to 4-4.
ous ; pearly on cl. Dark
verdigris-green to sky-blue ;
streak blue. C.c. : 62-6
copper protoxide, 30-3 ar-
senic tioid, 7'1 water. Corn-
wall, Tavistock, Erzgebixge.
425. MrxiTE.
Oblique prismatic or an-
orthic (?). Radiating, cen-
trally granular. osP 125°.
H. =3 to4;G. = 2-66. Eme-
rr-ld-green to blue-green ;
streak paler. C.c: 43-21,,. .„, , ._.. „. .-k / iat\
copper oride, 13 1 bismuth ^'8- «* (^- ^<'- ^- ^^5 (sp- 42*)-
oxide, 30-45 arsenic acid, 11-1 water. GeLstergang, JoachimsthaL
426. Rhaoite, 5Bij2i'3j-l-8Hj.
Grape-like groups of minute crystals. Colour yellowish green ;
streak white. Lustre wax-like ; brittle. H. =5 ; G. -6-82. C.c;
bismuth oxide 79-5, arsenic acid 15 '6, water 4-9. Neostadtel
near Schneeberg.
427. Tkooerite, 3iJlsj-fl2Hj.
Obliqiie prismatic, C 80°. Crystals thin tabular. Cl. clino-
diagonal, perfect. Lustre pearly. G. — 3 3. Lemon-yellow. C.c:
65-95 oxide of uranium, 17-56 arsenic acid, 16-49 water. In closed
tube gives off water, and becomes golden brown, but again yellow
on cooling. Neustadtel.
428. Stbuvite, (NH„ 2Mg) i?,-f I2H3.
Right prismatic. Poo (a) 63° 7', Poo (c) 96°, 4? 00 (J) 30° 32',
ooPa. (7.). JPco (m) 123°, OP (0) (fig.
436). Cl. brachydiagonal, perfect.
H. - 1 -5 to 2 ; G. - 1 -66 to 1 75. Trans-
parent or opaque ; vitreous. Colourless,
but yellow or brown. C.c: 29-9 phos-
phoric acid, 16-3 magnesia, 10-6 am-
monia, and 44 water. Under St Nicholas I
church at Hamburg, and in guano from
South America.
429. Arseniosideeite, sCaAsJ-^3feJA!3J-^6flJ.
Spherical and fibrous ; friable. H. -1-2 ; G. -3-52 to 8-88.
Opaque ; silky. Golden yellowish brown; streak yellowish brown.
C.c: peroxide of iron 39 4, lime IS'S, arsenic acid 87 9, water 8 9.
Romanfeche near Macon.
430. Chaloosiderite.
Anorthic Light green crystals. G. =3-11. C.c: 42-8 per-
oxide of iron, 8-1 oxide of
copper, 4-45 alumina,
30-64 phosphoric acid,
15 water. Cornwall.
431. Lazflite, AljPj
-KMg, fe)3iV2fi3.
Oblique prism.itic, C
88° 2'. ooP 91° 30', P (<)
99° 40', - P (p) 100° 20'.
Crystals often tabular
through distortion ; twins
on OP, and <»P°oo ; also
massive ; fracture splint-
eTo. -bto^S-l.^fran's- ^ig. 437 (.<p. 431).-\ /ig. 438 (sp. 431).
lucent ; vitreous. Indigo- and smalt-Wue to greenish ; streak
white. In closed tube yii-lJs water, and loses colour. Soluble in
acids after ignition. C.c: 3r7 alumina, 10 magnesia, -6 prot-
oxide of Iron, 44 phosphoric acid, and 8 water. Salzburg, Styria,
Brazil, (Jeorciu, Lincoln in North Carolina.
rig. 436.
MINERALOGY
407
Fig. 439.
432. CaiLDBEinTE,2(te,an),3f''+Al3(>'+16S. f-T^S-'U^kc.
Eight priamatic. Polar edges 101° 43', 130° 10', middle 98° 44';
nsual form P, 2f«o, ooPoo («, o, P, fig. 439).
H.-4-5 to 6; G.-318 to 33. Translacent ;
vitreous. Yellowiflh white to wine- or ochre-yellow,
brown, or almost black. Cct: 30,7 iron protojcide,
9 manganese protoxide, 14*6 alumina, 29 phos-
phoric acid, and 17 water. Tavistock, Crinnia
and Callington (Cornwall).
433. EosPHOBiTE (f'e, Jin)jil, ^+4fi.
Eight prismatic. P (p) 133° 32* and 118° 56'; ooP (i) 104° 19';
ooPco (a), oopco (*), oof 2 (g), 4? J (g), 2^2 (<) (polar edges 130° 26'
and 98° 42') (fig. 440). CI. macro-
diagonal. H.-6; G. -313. Pale
red. Vitreoua. C.c. : 22 alumina,
7 4 protoxide of iron, 23 '5 oxide of
manganese, 31*5 phosphoric acid,
16"8 water. Fairfield (Connecticut).
434. LiEOOONITE, Cuji's+'^lia
+ 24fi. J
Oblique prismatic, C 88° 33'. ooP
{d) 61° 31', P'oo (0)74° 21' (fig. 349).
H. -2 to 2-5; G. -2-8 to 3. Trans-
lucent ; vitreous or resinoua. Arure
blue to verdigria-green; streak paler
C.c: 366 protoxide of copper, 11-9
alumina, 26 '6 arsenic acid. 24 '9 water,
in Hungary.
435. Chalcophtllite, Cn5'is + 12fi.
Hexagonal rhombohedral ; E 69° 48' (fig. 441). CI. basal, perfect ;
sectile. H. -2 ; G. -24 to 26.
Transparent ; vitreous to adamantine.
Pearly on OE (</). Emerald- to grasa-
andverdigi'is-green; streak pale green.
Soluble in acids and ammonia. C.c: i .5. i^^.
protoxide of copper 49'6, arsenic acid 18, water 32'4. Eedruth
in Cornwall, Saida in Saxony, Moldawa in the Banat.
436. Ueanite, (Ca, e.) ''^ + &ii.
Eight prismatic. ooP'gO" 43'; P middle edge 127° 32'. OP : P
116-14; OP :2Pool09° 6'; OP : 2p«) 109*19' (figs. 442, 443). Crys-
tals flat. CI. basal, perfect; sectile. H. — 1
to 2; G. =3 to 3-2. Translucent; pearly on
OP. Sulphur- yellow to siskin-green; streak
yellow. C.c : 15*5 phosphoric acid, 62*6
uranium peroxide, 61 lime, and 15'8 water.
Fig. 440 (sp. 433).
Eedruth, Herrengrund
Fig. 442. Fig. 413.
Cornwall, Antun ami Limoges in France, Johann-Geoigenstadt
and Elbenstock in Saxony, Chesterfield iu Massachusetts.
437. Ubanospinite, (Ca, ej)&-H8S.
Eight prismatic; quadrangular, scale- like crystals. CI. basal,
perfect. H. ■= 2 3 ; G. - 3 45. Siskin-green. C. c. : lime 5 '47, sesqui-
«zide of uranium 69'18. arsenic acid 19-37, water 16'29. Neu-
stidtel.
438. UnAKOCIECiTE, (Ba, Bjp + sd.
Yellowish green crystals, isomorphous with 437. CL basal.
G. - 3 -53. C. c : sesquioxide of uranium 56 -86, baryta 14-57, phos-
phoric acid 15-1, water 14. Falkensteiu in Voigtland.
439. Chalcolite, (Cu, B.) PtSS.
Pyramidal. P middle edge 142° 8'; Poo 128° 14'. Crystals
OP, P, toPco , P« . CL basal, perfect ; pearly lustre ; brittle.
H. -2 to 2-5; G. — 3-5 to 3-fi. Grass- to emerald- or verdigris-
green; streak apple-green. C.c: 15-2 phosphoric acid, 61
uranium peroxide, 8-5 copper protoxide, and 15-3 water. Eed-
ruth and St Austell, Johann-Georgenstadt, Elbenstock, Schneeberg
Bodenmais, Baltimore.
440. ZELTfEKITE, (Cu, ISjis-f 8fi.
pyramidal. P middle edge 142° 6'. OP : P 109° 57'. Crystals
tabular. CI. basal. H. -2-5; G. -3-53. Grass-green. Lustre
pearly. C.c. : 77 oxide of copper, 55 '95 sesquioxide of uranium, 14
water. Huel Gorland in Cornwall, Neustadtel, Joachimsthal,
Zinnwald, Wittichen. •>.
441. WALPtjRoiTE, SBiis-hSSis-hlOfi..
Anor'Jiic; in scaly crystals. Wa.\-yellow to pomegranate-red.
Adamantine to greasy. H. -35; G. -.5-76. C. c : sesquioxide of
bismuth 60-4, sesquioxide of uranium 20-4, ai-senic acid 13, water
4 -5. Neustadtel.
442. Plombgomme, Pb,!? + 6ftUft,.
Reniform or stalaclitic ; fracture conchoidal and splintery. H. —
4 to 4-5; G.-6-3 to 6-4. Translucent; resinous. Yellowish' or
greenish white to reddish brown. C.c: 38 protoxide of lead 36
alumina, 8 nhosphoric acid, and 19 water, but with 2 chloride of
lead. Poulianouen, Nuissiere near Beanjeu), Georgia.
COMPODNDS OF PHOSPHATES, VaXADIATES, AN» AbsENIATBS
■WITH Haloid Salts.
443. Apatite, 3CaP'+Ca{a, F).
Hexagonal and pyramidal-hemihedric P 80° 26'. The most
common forms are ooP (M); t»P2(iO; 0P(m); P(a;); the base OP
seldom wanting (figs. 92, 95, 96, 97, 98). The ci7Stals are short-
prismatic or thick-tabular ; also granular, fibrous, or com-
pact ; fracture conchoidal or splintery ; brittle. H. = 6 •
G. -3-1 to 3-25. Transparent to opaque; vitreous to resinous.'
Colourless and white, but generally light green, grey, blue,
violet, or red. C.c: phosphate of liroo (89 to 92-3), with
chloride (to 11) or fluoride (to 7-7) of calcium, or both. Dissemi-
nated in granite, gneiss, mica and hornblende slates, primajy
limestones, and trap rocks ; also in beds and veins. Sutherland,
Rois, and Aberdeen, in granite and limestone; Cumberland]
Devonshire, and Cornwall; in tin-mines in Saxony; Bohemia'
St Gotthard, Tyrol; Kragero in Norway, New York, Canada.
441 Pybomoephite, 3Pb,-P'' + PbCl .
Hexagonal ; P 80° 44'. Crystals 00 P, OP, with' 00 P2, or P (it, P, x,
fig. 444), occasionally thicker in the middle, or spindle-shaped;
also reuiform or botryoidal ; fracture conchoidal or un- d
even. H. -35 to 4; G. -6-9 to 7. Translucent; resin-
.ous or vitreous. Colourless, but generally grass-, pis-
tachio-, olive-, or siskin-gieen, and clove- or hair-brown,
and scarlet (Leadhills). C.c: 89-7 phosphate and
10-3 chloride of lead, but with 0 to 9 arseniate of
lead, 0 to 11 phospliate of lime, and 0 to 1 fluoride of
calcium. Elgin, Wanlockhead, also Cornwall, Derby-
shire, Yorkshire, Durham, Cumberland, Wicklow ; ^'B- ^-'l-
Przibram, Mies, and Blcistadt in Bohemia ; Berezo'fl', Phoenixville
in Pennsylvania, and Mexico.
445. ViSADiNiTE, SPbj^ + PbCI.
HexaRonal; P 78° 46'. Forms c»P, OP (0), P(j), 2P, *P(M), o>P2,
00 Pi, 2P2 (fig. 445). Transparent to
opaque; resinous. Honey-yellow to
greyish brown; streak white. H. — 3;
G. -6-8to7-2. C.c:oxideoflead70-63,
vanadic acid 19-35, lead 7-2, chlorine
2-62. Wanlockhead, Windischkappel
in Carinthia, Haldenwirthshaus in
the Black Forest, Bolet in West-Got-
land, Berezovsk, Zimapan in ilexico,
Cordoba iu the Argentine Kenublic.
446. UiMETEsiTE, SPbsis + PbCI.
Hexagonal ; P 81° 48'. Crystals
ooP, OP, P (figs. 91, 444), or P, OP.
CI. P; fracture conchoidal or uneven.
H. -3-5 to 4; G. -719 to 725.
Translucent. Colourless, but usually
honey- or wax-yellow, yellowish green
rr grey. C.c: 90-7 arseniate and
9-3 chloride of lead; but part of the arsenic occasionally replaced by
phosphoric acid. Leadhills, Huel Alfred and Huel Unity in Corn-
wall, Roughten Gill and Dry Gill in Cumberland, Beeralston in
Devonshire, Jolianu-Georgeustadt, Zinnwald, Badenweiler, St
Prix iu France, Nertchiusk, and Zacatecas in Mexico.
447. Wacn-eeite, Mgji' + MgF.
Oblique prismatic, C C3° 25'. ooP 67° 35'. ' Cl. prismatic, and
orthodiagonal imperfect; fracture conchoidal or spliutery. H. — 5
to 5-5; G. —3 to 3-2. Translucent or transparent; i-esinous. Wine-
yellow and white C.c: 43-3 phosphoric acid, 11 4 fluorin*, 37-6
magnesia, and 7-7 magnesium ; but with 3 to 4-5 ii-on protoade
and 1 to 4 lime. Wcrfen iu Salzburg.
443. Teiplite, (Fe, iLOjJi + RF. -s^
Oblique prismatic ; only granular. Cl. in two directions at
right angles; fracture conchoidal. H. -5 to 6-S; G. -3-6 to 3-8.
Translucent or opaque; resinous. Chestnut- or blackish-brown;
streak yellowish grey. C.c: iron and manganese protoxides, with
83 phosphoric acid, and 7 or 8 fluorine. Limoges, Schlaggenwald.|
Fig. 445 (sp. 445).
408
MINERALOGY
449. ZviESELITE, (ifte, ^n)s¥' + FeF.
Right prismatic ? but only massive. CI. basal, perfect H. — 4*6
to 5; G. — 3'9B {o 4. Brown; streak yellow. (Xc. : like triplite.
Zwicsel in Bavaria.
450. Amblyoonite, 'id^P^ + (t\, iii)J^'f + &W, + (U, Na)F.
Anortliitr, crystals rare; coarse granular. CI. OP, pearly, meeting
t-.vo others at 105° and 87° 40'. Fracture uneven and splintery.
H. =»6; G. =-3to3"l. Translucent; vitreous. Greyish or greenish
white to pale mountain-green. C.c. : 47 '9 phosphoric acid, 34 '5
alumina, 69 lithia, 6 soda, and 8-3 fluorine. Penig, Arendal,
Montebras (Creuse, France), also Hebron and Paris in Maine.
M'jniabrasiCe has no soda.
451. DuEANGiTE, (R,)is + 2NaF.
Obliqus prismatic; crystals like keilhauite (.sp. 669). ooP 110° lO'j
P112°10'. CI. prismatic. H. -6; G. -3-95 to4. Bright orange-red;
streak cream-yellow. Vitreous. C.c: alumina 17 '2, iron protoxide
9 '2, arsenic acid 53, sod# 13 '1, fluorine 77. Durango (Mexico).
452. Hekderite.
Eight prismatic. P polar edges 77° 20' and 141° 16'; ooP 115°
53'. Fracture conchoidal. H. =6; G. =2-9to 3. Translucent;
vitreous, inclining to resinous. Yellowish or greenish white.
Ehrenfriedersdorf in Saxony. An anhydrous phosphate of alumina
with lime and fluorine.
Phospiiates with Sulphates and Bokates.
453. svanbergite.
Rhombohedral ; R 90° 35'. H. -=4'6; G. =2-67. Vitreous to
adamantine. Honey-yellow, reddish brown, and rose-red ; streak
reddish. Subtransparent. C.c: 37 '8 alumina, 6 lime, 17'3 sul-
phuri": acid, 12'8 soda, 17'8 phosphoric acid, 68 water. Horr-
sjbberg in Werraland.
454. DiADociiiTE, F'e3i';-H2FeS2-l-32H.
Reniform and stalactitic ; fracture conchoidal. H. «=S; G. *=1"9
to 2. Resinous ; vitreous. Yellow or yellowish brown; streak
white. C.c: 36"7 iron protoxide, 14"8 phosphoric acid, 16'2
sulphuric acid, 'and 30 '3 water. Gratenthal and Saalfeld.
455. PiTTiciTE, FejS3-l-2FeAs + 24H.
Reniform and stalactitic ; brittle; fracture conchoidal, H. =2"3;
G. ■='2"3 to 2 "5. Translucent throughout, or on the edges ; resinous
to vitreous. Yellowish, reddish, or blackish brown, sometimes in
spots or stripesj streak light yellow or "<vhite. C.c. : 35 iron per-
oxide, 26 arsenic acid, 14 sulphuric acid, and 24 water. In many
old mines, as Freiberg and Schneebcrg.
456. Beudantite.
Rhombohedral ; R 61" 18'. H. =3'6;G. =4. Vitreous. Olive-
green ; streak greenish yellow. C.c. : oxide of iron 40 "69, oxide of
lead 24-05, sulphuric acid 1376, phosphoric acidS'97, water 977.
Dernbach in Nassau, Cork in Ireland.
■JS7. LijNEBUROiTE (2Mg,'H) ?-t-MgB + 7H .
Concretions of fibrous structure. C.c: 25 '2 magnesia, 29 '83
phosphoric acid, 1474 boracic acid, 30*23 water. Liinehurg.
ARSENITES.
458. EoDEMiTE, Pb5'A3j-f'2PbClj.
Pyramidal, CI. OP. H. =2-5 to 3; G. =7-14. Pale green.
Vitreous on cleavage ; resinous on fracture. C.c: oxide of lead 69*67,
iead 22 2, arsonio'as acid 10 *59, chlorine 7*68. Ltogban in Wermland,
459, Trippkeite, Cuis,
Pyramidal; P 111° 56', Blue-green, Lustrous, Copiapo in Chili.
SILICATES.
Andalusite Group,
400, Andalusite, AlSi,
Right prismatic coP (m) 90° 60', Poo (r) 109° 4', Poo (s) 109° 51',
Fig, 416, Fig. 447.
Also columnar. CL m ; fracture splintery, H, - 7 to 7 B ; G, - 3 1 to
8*2, Pellucid; vitreous. Orey, green, red, or blue, B,B, infusible.
Not affected iy acids, Cc: alumina 63*1, silica 36*9. Clashnareo
(figs, 446 to 449) and Clova in Aberdeenshire, Mamoch and Botriph-
Fig, 448, Fig, 449,
nie in Banfi'shire, Killiney Bay in Wicklow, Andalusia, Tyro!
Penig, Massachusetts, Litchfield in Connecticut,
ChiastolUc. H. =5 to 5*5; G, =3, Pale grey, yellow, green, anc
red, A compound structure, formed of four double
wedge-shaped crystals, aiTanged in contact with the
angles of a square conoidal crystal placed in their
centre, and imbedded in a paste of clay slate. The
section of the compound structure forms a tesselated
cross, the appearance of which varies with the portion ^
of the crystal which is cut, Portsoy (fig. 450) and "S- «"•
Boharm in Banfi'shire, AVicklow, Keswick and Skidda-.v, Brittany,
Pyrenees, Maine, New Hampshire, Nova Scotia, Canada.
461. Ctanite (Disthene), AJS'i".
Anorthic ; generally broad-prismatic lengthened crystals, formed
by two faces (»n, t). m:t 106° 15';
m:»U5°41';iJ:m93°15'(fig, 451),
Hemitropes common, united by m.
Also radiated, Cl, m, perfect; brittle,
H, = 7, on cl. planes 5; 6, = 3 -5 to
3*7, Pellucid; vitreous, Cl, pearly.
Colourless, and red, yellow, green,
grey, and blue, B, B, infusible.
Kot affected by acids. C.c. same as
andalusite. Hillswick in Shetland,
Mount Battock, Tarfside (fig. 451),
Botriphnie (Banffshire), Tyrol, St
Gotthard, Bohemia, Ponti-.-y in
^^''°'^«* Fig. 451,
462. SiLLIMANITE, AlSi .
Right prismatic ; ooPlll°. Crystals fibrcap. columnar, and radi-
ating. CL macrodiagonaL H. -7; G. = 3*2 to 3*26. Translucent;
resinous ; on cl. vitreous. Greyish, gi*eenish, clove, or hair-brown.
C.c. and chemical characters like cyanite. Tvedestrand, Norway;
Chester and Norwich, Connecticut. Al203,Si02 is thusti*imoi-phous.
Jlonrohte, Xenoliie, Buchohite, Fihrolitc^ aud BamZiU are varieties.
463. Topaz, 6'ilSi -f AIF3 -h SiFj .
Right prismatic, ooP {U) 124° 17', 2?oo (n) 92° 42', ooP2 (I) OS"
14', P (0), Crystals always prismatic (fig, l'*!2), often hemimorphic.
Cl, basal, perfect ; fracture conchoidal, H, = 8 ; G, ■= 3 *4 to 3 'G.
Transparent ; vitreous. Colourless, honey-yellow, amber, pink,
asparagus-green, blue. Becomes electric by heat or friction, and
the yellow colours become pink, B, B, infusible. Not affected by
h, acid ; by digestion in s, acid gives traces of fluorine. The
formula requires 33*2 silica, 56*7 alumina, ]7*6 fluorine. Part of
the o.xygeu must be replaced by fluorine, as the total of the above
is 107*4. Ben-a-bourd and Arran, Scotland ; Mourne Mountains,
Ireland; St Michael's Mount, Cornwall; Siberia, Saxony, Bohemia,
Connecticut, Australia, Ceylon, Brazil, Peru. The finest topazes
are the blue from Scotland and Siberia, the pink, the yellow
from Brazil, and the colourless from Peru. The last-named when
cut may be distinguished at once from diamond by their elec-
tricity. PijrophysalUc is a massive opaque cleavable variety from
Falun. Pi/cnite is a columnar straw-yellow to "eddish white
variety from Zinnwald in Saxony /•
and Durango in ilcxico. f~^~T\
464. Staurolite, ('A'l,^F■e)gl-^(Fe, \^
J'lg) Si .
Eight prismatic. ooP(m) 128° 42',
Poo (r) 70° 46', ooPoo (0), of (^) (fig.
452). Twins common, as figs. 140,
144, 187, 453. Cl. brachydiagonal,
perfect ; fracture conchoidal to snlin- _> „ ,„
tory, H. -7; G. -3*6 to 8*8. Trans- F«- «2. (8p. 464.) F.g. 463.
parent to ojmque ; vitreous to resinous. Reddish brown : streak
white. B. B. iulusible. Kot atlected by h. acid, partially b/ s. acid«
MINERALOGY
409
C.c. : silica 30, alumina 485, with 5'S iron peroxide, I25 iron
protoxide, 3*5 magnesia ; often impure. Bixeter Voe and Unst in
Shetland, Boharm and Marnoch in Banffshire, StCotthard, Greiner
in Tyrol, Finistire, Urals, and Korth America. XanlholiU is a
jeilow variety from Urquhart (Inverness).
466. SAPrHiEiTE, 4Mg, 6iil, 2Si.
Oblique prismatic ; granular. H. — 7 to 8 ; G. — 3 4 to 8 5.
Titrcous; pale blue or green; translucent; dichroic. C.c. : alumina
63 2, magnesia 19 '3, silica 14 '9. Fiskenaes in Greenland.
ToURMAilNK GhODP.
466. TOUEMALINE, &,Si+fiSi.
Rhombohedral; E 133 10'. Crystals of OE (i'), -JR; usually
long prismatic, and striated (fig. 45, and 249 to 252). Generally
hemimorphic ; also radiating and fibrous ; fracture conchoidal to
uneven. H.— 6 5 to 7 5; G. —3 to 3'3. Black varieties opaque,
othera transparent ; vitreous. Generally black ; but colourless,
yellow, brown, blue, green, and rose-red ; streak white. Different
colours often disposed in layers parallel to the axis ; and
iwrtiona of one crystal differing also in colour along the
axis. By friction acquires positive electricity; and becomes elec-
trically polar when heated. Powder insol. in h. acid ; imperfectly
in s. acid. C.c. complex, but all with water and fluorine, some with
boracic acid. Coarse -black columnar varieties, called Schorl, very
common in granite and gneiss. Black occur at Portsoy in Banff,
Clova, Cabrach, and Rubislaw in Aberdeenshire, Bovey in Devon-
shire, St Just in Cornwall, in Greenland, Arendal, Tyrol, and North
America ; blue or IndiccliU at Utd in Sweden ; green at Glen Skiag
in Cromarty. Crystals ruby-red within , surrounded by green or red
at one extremity and green at the other, also blue and pink, at
Albany, Paris, and Hebron in Maine. Currant-red or Huhdliic in
India and Ceylon, also in Siberia and Brazil.
467. Datholite, OaB + CaSij-t-S.
Oblique prismatic, C 89° 51'. ooP (g) US' 22', ooP°2 (/) 76° 38',
P (/>) 120°, - P°oo (a) 45° 8', ooP»oo
<s), 2P«oo (o) (fig. 454) ; or rhombic
with J:/ 90°, b :o 135°, b:c 141° 9',
and /:y 160° 39'. Fracture uneven,
■OT conchoidal. H. =5 to 5'5 ; G. -=
2^9 to 3. Transparent or translucent ;
vitreous, Colourless and tinted gi-een-
ish, yellowish, or pink. In closed
tube yields water. B. B. intumesces
aud melts easily to a clear glass, colouring the flame green; the
powder gelatinizes in h. acid. C.c: 38'1 ^ica, 21 'S boracic acid,
Zi'l lime, and 5*6 water.
Bishopton in Renfrew, Glen
Farg in Perthshire (fig. 455),
Salisbury Crags and Corstor-
phine Hill near Edinburgh,
Arendal, Utb, Andreasberg,
Soisser Alp, Connecticut,
and Xew Jersey. Figs. 233,
239 are pseudomorphs of
quartz after datholite termed
Haytorite.
468. EucLASE, 2GlSi -)-
i'lH.
Oblique prismatic, C 79"
44'. o.P«2(j)115°;3P''S(/)
105° 49'. Crystals specially of 00 P«2, ojP'oo (r),3P'3. CI. clino-
diagoual, perfect; very brittle and fragile; fracture conchoidal.
Jb'lg. 454.
Fig. 455 (sp. 467).
Fig. 456.
■7-6; a -3 to 31.
Fig. 457.
Tianiparent ; iplendent ; ritreouj.
Fig. 458 (sp. 471).
Mountain-green, passing into blue, yellow, or colonrless. B.B.
intumesces, becomes white, and melts in thin splinters to a white
enamel. Not affected by acids. C.c: 42 silica, 36 alumina, 18
glncina, 6 water. Peru and Brazil, and Southern Urals. Cannot
be used as a gem on account of its brittleness ; whence its name.
469. HOMILITE.
Oblique prismatic, C 89° 21'. H.-SS; G.-8-28. Black and
brownish black. Vitreous. C.c: 27-28 lime, 1625 protoxide of
iron, 31-87 sihca, 18 1 boracic acid. Stokij aid Brevig (Norway).
470. BOTETOLITE.
Fine fibrous, botryoidal, «r reniform. Snow-white to hair-brown.
Chemical and physical characters like
datholite, but 10 64 of water,— being 2
equivalents. ArendaL
471. Gaiiolin:te, (i, Ce, f'e)jSi.
Oblique prismatic, C 89° 28'. ooP
116°; P 120° 56' (fig. 468). Fracture
conchoidal, or splintery. H. =6-5 to
7 ; G. =» 4 to 4-4. Translucent on the
edges; vitreous to resinous. Black;
streak greenish grey. -B.B. the con-
choidal (vitreous) varieties incandesce;
gelatinizes in h. acid. C.c: 36 to 51
yttria, 10 to 15 iron protoxide, 5 to 17 protoxide of cerium with
lanthanum, 0 to 12 glucina, and 25 to 29 silica. Hittero in Norway,
Ytterby, Broddbo and Finbo near Falun.
Epidote Geocp.
472. Zoisite, 4C8, 3itl, 6Si■^fi.
Right prismatic ooP 116° 26'; oop2 145° 24'; 00P3 156* 40'; Poo
122° 4'; 2Poo 111 6' (fig. 459). CI. brachydiag-
onal, perfect. H. - 6 ; G. - 3 '2 to 3 -4. White,
brownish grey, and dark green. B.B. intu-
mesces, and forms a white or yellow porous
mass ; and on the edges fuses to a clear glass.
C.c: 29-8 alumina, 24-35 lime, 2-8 oxide
of iron, 40-3 silica, and 2-1 water. Glen
Urquhart, Dalnain, and Allt Gonolan, In-
verness; Sterzing in Tyrol, the Sau Alp in
Carinthia, the Urals, and Connecticut
Thulite, peachblossom-red, from Souland in
Thelemai-k (Norway), is similar.
473. Epidote, 4Ca, 3A1, 6Si-HH.
Oblique prismatic, C 89° 27'. a.F°oo (it),
ooP 2 (0) 63° 1', P°oo (T) 64° 36', - P (n) 70°
25', - Poo (r) 63° 42', P (z) 70°. Crystals complex, with many
partial forms. Hemitropes united by T ; also columnar and granu-
lar. CI. if, perfect; also T, forming 115° 24'; fracture conchoidal
to splintery. H. -6 to 7 ; G. -3-2 to 3-5. Pellucid ; vitreous.
Green to yellowish grey.
B. B. fuses and swells to
a dark brown slag ; after
fusion soluble with gela-
tinization in h. acid.
C.c: 27-4 alumina, 85
iron peroxide, 23-9 lime,
38-3 silica, 19 water.
Shetland, Glenelginlnver-
ness, Tilquilly in Aber-
deen, in gneiss; in amyg-
daloid in Mull and Skye ; in granite at Cassencary in Kirkcud-
bright; Arendal, Dauphine, Greenland, the Urals, North America.
Wiihamite from Glencoe is a red, sti-ongly dichroic variety. Pierf-
mcflitiU or ifanr/anese Epidote, brownish violet, from St Marcel, haa
20 per cent, of manganese peroxide.
474. Allanite {Orthite, Cerine), ftjSij+SSi.
i j I
Fig. 459 (sp. 472).
Fig. 460.
Fig. 461.
Fig. 462.
Oblique prismatic, 0 65*.
Fig. 463.
oP («) 70° 48', P (n) 71'' 27', - P (<0
XYL — %2
410
MINERALOGY
96° iO', OP (if), P« (r), ooPoo (7). 31 : T 115°, T : n 111* 21',
J*: d 130° 18'. Often massive or granular; fracture conchoiJal. H.
-^ ; O. =» 3 '4 to 3 "8. Translucent on edges ; vitreous to resinous.
Black to brown or greenish ; streak brownish grey. B. B. froths
and melts to a brown glaas. Gelatinous with h. acid. C.c. : 12 to
IS alumina with peroxide of iron, 13 to 2(5 o.\ide of cerium and
lanthanum, 2 to 12 yttria, 4 to 20 protoxide of iron, 30 of silica.
Small crystals common in the syenitic granites of Scotland ; as at
Lairg, Boat of Garten (fig. 463), Aboyne, and Criffel. In lime-
stone at Urquhart (fig. 462), Greenland, Hitterb and Snarum,
Thuringia, Pennsylvania, New Jersey. Orthile (massive) at Ficbo,
Kragerb, and Falun. Cerine (granular) at Eiddarhyttan. fi/r-
orthite has carbonaceoas matter, Bodenite is a variety.
475. Idocrase, 3(Ca, MgjjSi + 2'A'lSi .
Pyramidal ; P (c) 74° 27' (figs. 464 to 466). Crystals
»P(d),
Fig. 464.
Fig. 465.
P2 if). Prismatic,
' 6-5 J
ooPoo (if), P (c), OP {p). Poo (o) 56° 29';
striated ; also granular ; fracture uneven.
G. = 3 '36 to 4. Pellucid ; vitreous to resinous. Brown,
green, yellow; Btreak white. B.B. fuses easily, with
intumescence, to a green or brown glass. Partially
sol. in h. acid ; after ignition totally, gelatinizing.
C.c. : alumina 16, peroxide of iron 7, lime 34, silica
38. Glen Gnirn and Crathie, Aberdeenshii-e, in lime-
stone ; Broadford, Skye j Wicklow and Donegal, Ire-
land ; Egg, Norway ; Mussa, Piedmont ; Vesuvius ; F'g- 466.
Wilui river, near Lake Baikal (fig. 463). Cypriiie from Thele-
mark is azure-blue, from copper.
Olivine Gkocp
476. FORSTEBITE, llgj. Si.
Right prismatic. Like olivine (sp. 478). H. = 6 to 7 ; G. = 3 -2 to
3 '3. Vitreous ; transparent. White, wa.x-
yellow, greenish ; streak white. C.c. :
magnesia 57'1, silica 42-86. Vesuvius.
Soltonite, red, is from Massachusetts.
477. Fatalite, Fe.Si.
Eight prismatic ; n:n' 49° 36' (fig. 467).
Massive. CI. reotanguLir. Black, green-
ish, or brownish. Slctallic to resinous ;
fracture conchoidal ; magnetic. H. = 6"5;
G. = 4 to 4*1. C.c. : protoxide of iron
70», silica 29 '5. Mourue Mountains,
Ireland ; Fayal, Azores.
478. Chrysolite (Oliviiie, Peridotc),
(Fe lilg)2Si .
Right prismatic. P {c) 85° 16' and ^8- ^" ''?■ ■''^•
139° 54' ; middle 108° 30'. odP (n) 130° 2', Poo (<i)76° 54', 2poo
(h) 80° 63', ooPoo (j)/) (fig. 468). Also massive. CI. brachy-
diagonal, perfect ; fractui'e conchoidal.
H.=0-6 to 7; G.-3-3 to SB. Traus-
parent ; vitreous. Olive-greon, yellow,
brown, and colourless. B.B. infusible.
Soluble, with gelatiuijcing, in acids. C.c. :
47 magnesia, 12 protoxide of iron, 40
silica. Taliskcr in Skye, Haalival in
Eum, Elie in Fife, Unkel on the Rhine,
Vesuvius, Esnoh in EgTOt, Brazil. Bya-
losidiriU, brown an<l yellow, with metallic
lustre and 30 per cent, protoxida of iron,
is from the Kaiserstuhl in the Broisgau.
479. Tephboite, MnjSi. Fig. 468 (sp. 478).
Right prismatic ; granular, with rectangular cleavages. Ash-
grey, rose-red- Adamantine; translucent. H. — 5 '5 to 6; G. — 4
to 4-1. C.c, : protoxide of manganese 70 2, silica 29 'S. Franklin
and Sparta in New Jetsey.
480. Kkebellite, tc^i •»■ fin^Si .
Massive. Grey, brown, green, black. Glistening ; brittle.
H. -6-6; G. -S-71. C.c: protoxide of iron 355, protoxide of
manganese 35, silica 29*5. flmenau, Dannemora in Sweden.
481. MoNTIOELLlTE, Ca^i -h MgjSi .
Eight prismatic. P (/) 110° 43' and 97° 55', aP (s) 98° 7", ocP2
{n) 133° 6', f «> (fc) 81° 57', JPoo (h) 120° 8', P2 (e) 141° 47' and 82°,
CO Poo (6) (fig. 469). Vitreous. Grey,
yellowish and greenish, and white ;
streak white. Translucent. H. =5
to 5-5; G. -3 to 3-25. C.c. : lime 35,
magnesia 21 '9, protoxide of iron 5*6,
silica 37 '5. Sol in h. acid, gelatiniz-
ing. Somma (Milan).
482. Chondeodite (HumiU),
ligjSij.
Right prismatic. P middle edge
156° 38', polar edges 131° 34' and
54° 28' (figs, 470 to 472). Crystals
monoclinio in habit, often granular-
massive. H.=C-5;G.-315to3-25.
Translucent ; vitreous to resinous. Yellow, red, brown, green, and
black ; streak white. B. B. infusible. Decomposed by acids. C.c:
Fig. 469 (sp. 481).
Fig. 470.
Fig. 471.
Fig. 472.
silicate of magnesia, with 2 to 3 of fluorine. From limestone on
Loch Ness (?); Pargas, Finland; Gallsjb and Aker, Sweden : New
York ; Sparta, New Jersey. SumiU, from Somma.
483. LlEVRITE, 3(Fe, CajjSi-l-FeSi-fff.
Eight prismatic. P (o) polar edges 139° 30' and 117° 27' ; ooP
112° 38', Poo {d) 112° 49', ooP2 (s) 106° 15'. Crystals (fig. 124) are
long-prismatic and vertically striated ; also rpidiated, columnar, or
fibrous; brittle. H. =5*5 to 6; G. «= 3 '9 to 4 '2. Opaque ; resinous
or imperfect metallic. Brownish or greenish black ; streak black.
B.B. fuses easily to a black magnetic globule. Sol, in h. acid,
forming a yellow jelly. C.c. : 29-3 silica, 196 iron peroxide, 35-2
iron protoxide, 137 lime, and 2*2 water. Rio iu Elba, Fossnm,
Kupferberg, Rhode Island, and Greenland.
484. CEiiiTE(Ce, ft),Si-HH.
Hexagonal ; OP; ooP; in low six-sided prisms. Generally fine-
granular ; fracture uneven, splintery ; brittle. H. =5*5; G. = 4*9
to 5. Translucent on the edges ; dull, adamantine, or resinous.
Clove-brown, cherry-red, or pcarl-grcy. Sol. in h. acid, leaving
gelatinous silica. C.c: 20"5 silica, 73'5 proto?dde of cerium (with
didymium and lanthanum), and 6 water. Bastnacs near Eiddar-
hyttan.
485. Galmei, 2nJSi■^S.
Right prismatic, and hemimorphic ; 2? 2 (P) with polar edges
101° 35' and 132° 26', ooP (rf) 103° 50', Poo (o) 117° 14', Pco (?)
128° 55' (fig. 40) ; common form ooPoo (s), ooP, Poo. Also
columnar, fibrous, granular, and earthy. CI. prismatic along ooP,
very perfect; along Poo perfect, H. = 5 ; G, — 3'3 to 3"5. Trans-
{iarent to translucent ; vitreous and peaily. Colourless or white,
)ut often light grey, also yellow, green, brown, ajid blue ; becomes
electric by heat. B.B. decrepitates slightly, but is infusible ; with
cobalt solution blue and partly green ; rtadily soluble iu acids, and
gch-itinizes. C.c : 25 silica, 67 5 zinc oxide, and 7 5 water, Wnn-
lockhcad, Mcndip Hills, Matlock, R.nibl and Bleibcrg in Carinthi^
Aix-la-Chapelle, Iscrlohn, Nertchinsk. Pennsylvania, Virginia.
Used as an ore of zinc.
Willemite Gkoup.
486. 'Willemite, t-a^i.
Rhombohcdral ; R 116° 1'. CI. basal, and prismatic, ooR ;
orittlc. H, - 6 -5 ; O, - S 9 to 4 '2, White, yellow, brown, and red.
Vitrojus lustre. C.c. : oxide of zinc 73, silica 27. Altenbei;^
Liege, GnciUaud. New Jemy.
MINERALOGY
411
^ST.'Tboostite, 2nSi + iiBSi.
yRhombohedral ; R 116'. a. prism&tic, ooP2 ; brittle. H. -5-5;
G. — 4'1. Asparagus-green, grey, and reddish brown. Vitreous.
C.c. : oxide of zinc 53, oxide of manganese 13, silica 28. New Jersey.
488. Ckntbolite (f bMn) Si .
Eight prismatic; ooP. 115° 18'. Form ooP, P, oopoo. H. -6;
G. -6 2. Eed-bxowD- CI. prismatio ; splendent on P. Southern
Chili.
489. Phekaoite, CiljSi.
Hexagonal and tetartohcdral ; E (p) 116° 36' (fig. 478). Crystala
K, a>P2, JP2. Twins with
parallel axes, and intersecting.
CI. E, and ooP2 ; fracture con-
choidal. H. =75 to 8; G. -=
2 ■97. Transparent or trans-
lucent ; vitreous. Colourless,
and wine-yellow or brown when
fresh, but colour soon lost on
Fig. 473 (sp. 489).
= 3 '2 to 3 -3. Transparent or
Fig. 47-4 (sp. 490).
exposure. B. B. infusible; not
affected by acids. C.c. :glucina
45 '8, silica 64 '2. Framont in
Alsace, Takovaya in Urals,
Miask, Burango in Mexico.
490. DioPTASE, CuSi + fi.
Hexagonal and rhombohe-
dral ; R 125° 64', t 2R (r) 95°
28', a.P2, - 2RJ (») (fig. 474).
CI. R, perfect ; brittle. H. = 5;G.
translucent; vitreous. Emerald-green, rarely verdigris-green or
blackish green; streak green. C.c. ; 38 7
silica, 50 copper protoxide, and H'3 water.
Altyn-Tubeh in the Kirghiz Steppe, Murosh-
naya, Copiapo.
491. Chrtsocolla, CuSW2S.
Botryoidal or investing ; brittle ; fracture
conchoidal. H. = 2 to 3 ; G. = 2 to 2 -3. Trans-
lucent ; resinous. Verdigi-is- to emerald-green
or azure-blue ; streak greenish whifo. C.c:
34*83 silica, 44'94 copper protoxide, and 20*23
watei*. Leadliills, Lackentyre in Kirkcud-
bright, Cornwall, Saxony, Hungary, Spain,
Urals, Australia, Chili.
492. EoGOSLOVSKiTE (Sup/erilau).
Massive; fracture conchoidal; brittle. H. =
4 to 5 ; G. = 2 -66. Sky- to ultramarine-blue ;
streak smalt-blue, and shining. A silicate of
copper, with 46*5 per cent, copper oxide. Schapbach Valley in
Baden, Bogoslovsk in the Urals. Danidowitc may be the same.
Gaknet Group.
493. Garnet, ft^Sij-t-S'Si.
Cubic ; most common forms cxiQ and 202 (figs. 33, 40, 60, 475).
Also granular. CI. dodecahedrnl ; fracture conchoidal, or splintery
H.-6*5to 7*5;G.-3*6 to 4*3. Pellucid;
vitreous or resinous. Rarely colourless or
white ; generally red, brown, black, green, or
yellow. B. B. in general fuses to a glass, black
or grey in those containing much iron, green
or brown in the others, and often magnetic;
imperfectly soluble in h. acid. C.c. ex-
ceedingly variable, but generally forming two
series, according as 'R.,0.^ is chiefly alnmina or
chiefly iron peroxide "; and these are again Fig. 475.
divided according as RO, is more especially lime, iron pro-
toxide, magnesia, or a similar base. The more important varieties
are —
(1) Livie- Alumina Qamel, (JajSu -^ ilSi, with 40 silica, 23
alumina, and 37 lime. To this subdivision belong —
(a) /ro/erffanirf.— Colourless to white. Craig Mohr, Aberdeen ;
Thelemark in Norway.
(6) Grossular. —Olive- to gooseberry-green. Craig Mohr : Wilui
river ; America.
(c) Cinnamon S(o»«. —Hyacinth-red to orange-yellow. Glen
Gaim (Aberdeen), Allt Gonolan and Ord Ban (Inverness), Ceylon,
W*rmland. Itommttowite, from Kimito (Finland), is the same.
This variety when polished is often sold as Hyacinth.
(d) Common Lime Ganut.—HeTe one half of the alumina is
replaced by iron peroxide. Colours red.'brown, yellow. Piedmont
Vesuvius, the Urals.
-(2) Magnesia-Alumina Garnet : RO chiefly magnesia. Arendal.
(Z) Manganese- Alumina Camel; RO-MnO; reddiah-brown.
Spessart (Bavaria), Sweden.
(4) Magnesia-Iron-Zime-Alumina Garnet, Pyrope. — Colour port-
wine to purplish red. Elie in Fife, Zdblitz in Saxony, Bohemia.
(5) Iron-Alumina Garnet, Almandine, Noble Garnet. — Colum-
bine-red, inclining to violet, blood-red, and reddish brown.
Common in mica-slate, gneiss, and granite. Shetland, Ross,
Inverness, Aberdeen, Falun, Arendal, Tyrol, the Urals, North
America, Pegu, and Ceylon.
(6) Lime-Clirome-Alumina Qarrut, CajSi,-f ('6r, •il)§i, UwarO'
wite. Emerald-green ; with 22 per cent chrome oxide. Bissersk
and Kyshtimsk in the Urals, India, and California.
(7) Lime and Iron Garnet, CajSij + Fe, Si. This includes —
(a) Common Iron-GariKt, RothoJjiU, Allochroile. — Subtranslucent
or opaque. Green, brown, yellow, or black; with white, grey, or
yellow streak. Sweden and Arendal.
(6) Melanite. — Black ; opaque ; in thin splinters translucent ;
streak grey ; slightly magnetic. Albano near Frascati, Vesuvius,
France, Lappmark.
(c) Colophonile. — Yellowish-brown to pitch-black, also yellow or
red; resinous; streak white. G. = 3*43. ArendaL
The red varieties, when cut en cahochon, are termed Carbuncles^
494. AxiNiTE, (iA, 'li) Si-l-2(Ca, te)Si.
Anorthic. Crystals unsymmetrical. u : P 135° 31'; «:r 115°
38', P:r 134° 45' (figs. 136, 137). CI. distinct along planes tnin-
catingthe sharp edges between P ■and « andP and r. H. =6*5
to7i G. = 3*2 to3*3. Pellucid; vitreous. Clove-brown, inclining to
smoke-grey or plum-blue; but often cinnamon-brown in one direc-
tion, dark violet-blue in a second, and pale olive-green ra a third
{trichroism). B.B. colours flame green; intumesces, and fuses easily
to a dark green glass, becoming black in the ox. flame ; not sol. in li.
acid till after ignition, when it gelatinizes. C.c: 45*9 silica, 5*9
boracic acid, 17*5 alumina, 9*3 iron (with manganese) protoxide,
and 21*4 lime. Botallack and other mines in Cornwall, Bourg
d'Oisans in Dauphine, Kongsberg, Aiendal, Nordmark in Sweden,
Pyrenees, St Gotthard, Tyrol, Thura in Saxony, Urals, and North
America.
495. Danbubite (Oa, B) 2Si .
Right prismatic. ooP {I) 122° 62', oof 2 (e) 94° 52', P«> (d) 97*
7', 4f 00 (w) 54° 58', OP (c), P (o), 2P2 (r), oopoo (a), o>f 4 (n).
f^^r^
Fig. 476.
Fig. 477.
Fig. 478.
Fig. 479.
Gl. basal ; fracture uneven to subconchoidal ; vitreous to greasy
lustre. H. -7 to 7*5; G. =2*986 to 3021. Pale yellow to reddish
brown. Translucent ; brittle. C.c: 22*76 lime, 28*46 boiacic acid,
48*76 silica. Danbury in Connecticut, Russell in New York.
Helvine Geoitp.
496. Helvine, MnS-^3K2Si.
Cubic and tetrahedraL "o* or "o* ~ T '*'*'■ '^ ^""^ ''"' ^^'" ""■
bedded or attached. CI. octahedral. H. = 6 to 6*5; G. = 31 to
3 "3. Translucent on the edges ; resinous. Wax-yellow, siskin-
green, or yellowish brown. B. B. in the red. flame fuses with in-
tumescence to a yellow obscure pearl ; sol. in h. acid, evolving
sulphuretted hydrogen, and gelatinizes. C.c. : 34 silica, 10 glucina,
8 iron protoxide, 43 manganese protoxide, and 6 sulphur. Schwarz-
enberg in Saxony, and near Modum in Norway.
497. Dakalite, SftjSi + ZnS.
Cubic. In octahedra, with striated dodecahedral planes. H. = 6*6
to 6 ; G. =3*43. Vitreous to resinous. Flesh-red to grey ; streak
lighter. Translucent ; brittle. C.c. ; protoxide of iron 29, of
manganese 6*5, of zinc 19, silica 31*6, sulphur 6*5. Eockport
in Massachusetts.
498. Edlttine, BijSia .
Cubic and tetrahedral. ?5? and -?2?. The crystals (fig. 66)
small, and often \vith curved faces ; fracture conchoidal. H. = 4*6
to 5; G. =5*9 to 6*1. Transparent and translucent; adamantine.
Clove-brown, yellow, grey, or white; streak white or grey. C.c:
16*2 silica and 83*8 bismuth peroxide. Schneeberg and Brauns-
dorf near Freiberg.
412
MINERALOGY
ScAPo:.iTE Gnour.
;59. Sarcdlite, SCa, S'l^l, Ni, 9Si,
Pjiamidal. P 102° 64'; ooPoo ; OP; P, and other faces as in fig.
480, many of the faces being alternately hemiliedral. H. =5'5
to 6 ; G. — 2'93. Vitreous. Grey to rose-red. Translucent; very
brittle, C.C.: alumina 21 '5, lime 32'4, soda .3-3, silica 40'6.
B. B. f)i6Q3 to a whit^ enamel; gelatinises with acids. Somma.
Kg. 480 (sp. 499).
Fig, 481 (sp 500).
600. MziONiTE, 6(da, Na), 4A1, 9Si .
W; "P (»);
P (5) (fig. 481)
Pyramidal. P (o) 63° 42'; Pc
CI. macrodiagonal. H. = 5 £ to 6;G. = 2-6
to 2 '74. Vitreous. Colourless or white.
Transparent. Much cracked. Co.: 31 '9
alumina, 26 '2 lime, 41 '9 silica. Gelatinizes
in acids. Somma.
601. MizzONiTE, 6(Ca, fei), 4^, 15Si.
Pyramidal; P 64° 4' (fig. 482). Similar to
meionite. C. c. : alumina 23 '8, lime 8 *8,
soda 9'8, silica 547. Insoluble in b. acid.
Somma.
502. SOAPOLITE, 3(Ca, S a)6i +'Al28i, . ''■& ^^2 (sp. 601).
Pyramidal P 63° 42' ; ooPoo ; P ; cbP ; also massive. CI.
coPoo, perfect; and ooP. H.-5 to 6-5; G.-2-6 to 2-8. Trans-
parent or translucent ; vitreous, pearly, or resinous. Colourless, but
also pale grey, green, yellow, or red. B. B. melts with etfervescence
to a vesicular gla.ss; in the closed tube may show traces of fluorine;
with solution of cobalt becomes blue. SoL in h. acid. C. c. : 49
silica, 28 alumina (with iron peroxide), and 23 lime (with soda).
Tiree (Scotland), Arondal, Tunaberg, Pargas, Massachusetts, and
New York. Known by its rectangular cleavage, resinous lustre on
fractured surfaces, and action B. B. Dipyre, P 64° 4', is a variety.
603. Uelulit-b (ffumloldtilik), 2((!;a, Mg)Si-,-f('il, Pe)Si
Pyramidal. P 65° 30'; OP; ooPm. CL basal, perfect. H. -5
to 6-6; G. =2 '91 to 2 '95. Translucent on edges ; vitreous to resin-
ous. Koney-yellow, orange-brown, and yello^vish white. C. c. :
32 lime, 7 magnesia, 9 alumina, 7 iron peroxide, 40 silica. Capo
di Hove, and Vesuvius.
604. Gehlenite, (Ca, Fe)sSi -1- (Al, 'Fe)Si .
Pyramidal. P. 69° ; OP; ooPco ; ooPS; 2P. CL basal. H. =6'5
to 6 ; G. -2'9 to S'l. Translucent on edges. Dull resinous.
Mountain-, leek-, or olive-green, and liver-brown. C. c. : 22
alumina, 5 iron peroxide, 35 lime, 4 magnesia, 31 '4 silica. Mon-
2oui in the Fassa Valley.
NErHEUtTE Group
606. Ledoite, 'AJ, Sij -(• KS'i
Pyramidal. Combination of the ditctragonal pyramid (0 with the
tetragonal pyramid'o), and 2Poo (B)with ooP(m). Hemitropes united
Fig. 483.
Fig. 484.
by (u). Fracture conchoidal. H. -6'5 to 6; G. -2-4 to2-6. Trans-
parent to translucent on the edges; vitreous, inclining to resinous.
Colourless, but greyish, yellowish, or reddiah white ; atrcok white.
B.B. infarible ; with cobalt solution becomes blue. Sol. in h.
Fig. 485.
acid, without gelatinizing. C.:.: 54 9 ;i!ica, 23-6 alumina, and
21 '6 potash. Abundant m the lavas of Vesuvius, the tufas near
Rome, and the peperino of Albano ; d.ho at the Kaiserstuhl, and
near Lake Laach. Readily distinguished from analcime by its in-
fusibility, and by never showing faces of the cube.
506. Nepheline {Elesoliie), AlSi + 4(Na, S)Si .
Hexagonal. P 88° 10'. ooP, OP, P common ; also fig. 485.
Crystals imbedded, or in dmses ; also
massive-granular; fracture conchoidal,
oruneven. H.-6'5to 6; G.-2-58
to 2 '64. Transparent or translucent ;
vitreous and resinous. Colourless or
white (nepheline) ; or opaque, dull
resinous, and oreen, red, or brown
(cl.-eolite). B^B. melts difficultly
(nepheline), or easily with slight effer-
vescence (elseolite), into a vesicular
glass. Sol. and gelatinizes in h. acid.
C.c. : 41-2 silica, 35-3 alumii
soda, 6 '5 potash. Nepheline at Monte I
Somma, Capo di Bove, Katzenbuckel
in the Odenwald, Aussig, and Lusatia.
Elaiolite in the zircon syenite at Laur-
vig, Fredriksvarn, Brevig, and iliask.
havi-ne, with \V 51° 46', seems only a variety; as also Cancri-
nite, bright blue, and with some carbonate of lime.
607. MiCKOsoMMiTE, RSi -l- AlSi + NaCl .
Hexagonal. ooP;OP; c»P2;»P?. CI. ooP. H.-6;G.-2-42
to 2 ■53. ' Colourless to yellow; lustre silky. Somma and Vesovlna.
508. SoDALiTE, 3(ilSi-hJ!fa§i)-(-NaCl.
Cubic ; ooO, and fig. 486 ; generally distorted ; also massive and
granular. CI. ooQ ; fracture
conchoidal or uneven. H. —
6 -5 ; G. - 2 -13 to 2 -29. Trans-
lucent; vitreous. Wliite, grey,
and rarely green or blue. C.c:
37 silica, 31-8 alumina, 19-2
soda, 4 '7 sodium, and 7 '3 chlo-
rine. Greenland, Vesuvius,
Ilmen Hills, Fredriksvarn, and
Litchfield in Maine.
509. NosEAN, 3(AlSi -I- NaSi)
■fNaS.
Cubic ; and granular. H. «=
5-5; G. -2-28 to 2-40. Trans- ^^
lucent ; vitreous to resinous. '= " ^ y "««/•
Ash or yellowish grey, sometimes blue, brown, or black. C.c: 36
silica, 31 alumina, 25 soda, and 8 sulphuric acid. Lake I^aacb,
and Rieden near Andernach. on the Rlune. Occurs in phonolites,
in minute crystals.
510. IlATnr^^E, 2(A^lSi + ^aS*i) + CaS'.
Cubic; chiefly odO ; also fig. 487; but more common in grains.
Ch coO. H. -5 to 5-5; G. ™2-4 to 2'5. Semitransparent or trans-
lucent; vitreous or resinous. Azure- or
sky-blue; streak bluish white. C.c: 34'2
silica, 28 5 alumina, 11*5 soda, 4'3 potash,
10 '4 lime, jud 11 '1 sulphuric acid. Vesu-
vius, Mount Vultur near Melfi, the Cam-
pagna of Rome, and Niedermendig near
Andernach
611. Lapis-Lazi'LI.
Cubic ; Ooo ; generally massive, granu-
lar. H. -6-5; G. -2-38 to 2-42. Trans- Fig. 487 (sp. 610).
lucent on edges; dull resinous or vitreous. Ultramarine, or
azure-blue; streak light blue. B.B. fuses readily to a white
porous glass. In h. acid the powder is dissolved and gelatinizes,
evolving sulphuretted hydrogen. C.c: 45-50 silica, 5-89 sul-
phuric acid, 3176 alumina, 9 09 soda, 3-62 lime, 0 86 iron, 042
chlorine, 095 sulphur, 0-12 water. Near Lake Baikal, China,
Tibet, Tartary, Monte Somma, and Chili. It is used for ornamen-
tal purposes, and in the preparation of ultramarine. The colour
both in it and hauyne seems duo to some compound of sulphur
with sodium and iron.
Mica Group.
512. BiOTlTE (iV(ii7Ji«ia-ifiM), 'AVsia-t-iSlg, K, ^6)3813.
Oblique prismatic, C 89* 69'. OP (c), 98° 41' P (m), - JP (0),
a>P^oo(6).^co(r), - jP«3{r). CI. basal, perfect; scctilo; thin plate*
clastic. H. -26 to 3; G. -2-86 to 2 -9. Transparont, but often only
MINEKALOGY
413
in very thin plates. Generally uniaxal, sometimes with diver-
gence—66". Metallic, pearly. Usually dark green, brown, or black ;
streak CTcenish grey or white. B. B. difficultly fusible to a grey or
black ^asB. Completely soL in concentrated s. acid, leaving white
Fig. 488. Fig. 489.
pearly plates of silica. Co. : 39 silic.i, 17 alumina, 10 iron protoxide,
20 magnesia, 9 potash. Hillswick, Shetland, in gneiss; Sutherland,
lloss, Inverness, in limestone; Skye and Fife in trap; Pargas, Boden-
mais, Greenland, New York. Ruidlan is a decomposed variety.
613. Hacghtonite, ('Al,!Fe) Si + (Fe, 8)281.
Oblique prismatic. CI. basal, perfect. H. — 3; G. —S'l. Vitreous
to adamantine. Chocolate-brown to black. Weathers pale green
end ochry. Difficultly soluble in acids. B.B. fused with difficulty
to a highly magnetic bead. C. c. : silica 36, alumina 18, ferric oxide
4 5, ferrous oxide 18, magnesia 9, potash 8, water 3. Common in
the granites of Scotland. Black Forest, Harzburg, Tyrberger.
614. Lepidomelane, (Al,3p'e) Si + (fe, K)Si.
Oblique prismatic. CI. basal, perfect ; "brittle. H. =3; G. =2-97.
Vitreous; transparent to opaque. Rich brown to raven-black.
B.B. fuses easily to a blacK feebly-magnetic bead. Sol. in h.
acid, leaving pearly scales of silica. C.c. ; 37 silica, 37 alumina, 24
ii-on peroxide, 3 protoxide of iron, 8 potash, 10 magnesia, 4 water.
Rarely in gneiss, Scotland ; common in granite, Ireland; and Pers-
berg, Sweden.
616. Anomite, 12ilg, 3JU, 2S, fi, 12Si.
Oblique prismatic, c :m 98° 42'. Form c, m, 0, 6 (see fig. 488);
divergence of optic axes 12° to 16°. Monroe (New York), Lake Baikal.
616. Phlooopite, (IR3 ■^ jS) Sij .
Oblique prismatic. OP (c), P (m), - JP (0), ooPoo (J), e : m 98° 30'
to 99°. CI. basal, perfect H. -25 to 3; G. -276 to 2-97. Pearly
to submetallic. Yellowish brown with copper-like reflexion; also
green, white, and colourless. Transparent. Divergence of optic
axes 3° to 20°. C.c: 14 alumina, 2 protoxide of iron, 28 mag-
nesia, 8"6 potash, 2'57 fluorine, 41 silica. B.B. whitens, andfuses
30 edges. Decomposed by s. acid, leaving the silica in scales.
Pargas (Finland), Fassa Valley, New York, Canada, Ceylon. Char-
acteristic of serpentine and of dolomitic limestones.
517. ZiNNWALDITE.
Oblique prismatic. Forms as in figs. 490, 491 ; also 2Poo {H) and
SP'S (x). m : c 98° to 99°. Divergence of optic axes 65°. G. -
282 to 3'2. C.c. similar to muscovite (sp. 619), but with 4 to
Fig. 490. Fig. 491.
8 fluorine, 2 to 5 lithia, and traces of rubidium, cxsiam, and thal-
lium. Altenberg and Zinnwald, St Just and Trewavas in Cornwall.
CnjophylliU from Cape Ann in Massachusetts is similar.
518. Lepidolite.
Oblique prismatic. Forms like muscovite. Divergence of optic
«es 50^ to 77°. CI. basal, perfect. H. =2-6 to 4; G. -2-84 to 3.
Often massive; scaly granular, coarse or fine. Lustre pearly. Colour
fose-red, violet, lilac, yellow, greyish white. Contains 5 to 6 per
■;ent. lithia, with rubidium, csesium, and thallium, also fluorine.
B. B. colours flame red. Mourne Mountains, Rozena (Moravia), Uto
(Sweden), Ekaterinburg, Maine.
519. UvscoviTE (Muscovy-Olasa), 3i'lSi-(-KSi.
Right prismatic, with monoclinic habit. 0P(c); a-F {^t)■, ooP'co
(i); P (m); 2P«oo (j/). ooP nearly 120°. Twin-face e. CI. basal,
perfect ; elastic. Angle of optic di-
vergence from 44° to 77°. Metallic,
pearly. Colourless, and tinged of
various shades to black. B. B. fuses to
an opaque enamel. Not affected by
acids. C.c: 36-6 altlmina, H-8 pot-
ash, 46 '1 silica, 4*5 water, with traces
of fluoi-ine. Shetland, Loch Glass in Sutherland, Glen Skiag
(crystals 16 inches in length) and Struay Bridge in Ross, Aber-
Fig. 492.
deen, Cornwall, St Gotthard, Norway, Sweden, Siberia. Crystals
over a yard in diameter in China, where it is used for windows.
Fuchitc, bright green, has 6 per cent, of chrome oxide. Mcirgaro-
dite contains 4 to 6 water. Qilberlite, Cornwall, may be different.
620. Paragokite (Soda-Mim), sAl^Sij -t- (Jja, fi)Si .
Massive; foliated. Lustre pearly. H. =2-5 to 3 ; G. -278 to2'9.
Yellowish, greyish, and greenish. C.c: 40-1 alnmina, 6-1 soda,
4775 silica, 4-6 water. Monte Campioue, St Gotthard.
521. Sandbeeoerite {Baryta- Mica).
White minute scaled aggregates. G. -2-894. C.c : 30 '2 alumina,
4-9 mao;nesia, 6'9 baryta, 7-6 pot-ash, 42-6 silica, 4-43 water.
Pfitsch Valley in Tyrol, aud the Swiss Alps.
522. Maroarite {Lime-Mica).
Right prismatic. CI. basal perfect. H. =3 5 to 4-6; G. =2 '99 to
3'1. Lustre of cl. pearly. Lateral planes, vitreous. Snow-white,
reddish white, and pearl-grey. Lamina; brittle. Optic axial
angle 109° to 129°. C.c : 61;2 alumina, 11-6 lime, 2-6 soda, 30-1
silica, and 4 5 water. Greiner in Tyrol, Naxos, Asia Minor, Greece,
Pennsylvania, North Carolina. Diphanitc is similar.
523. Euphyllite (Jftj + iti)^!, + jS .
Like muscovite, but lamince not easily separable. H.=3'5to4'5;
G. — 2'83 to 3. Lustre of el. pearly to adamantine. White to
colourless. Transparent to opaque. Laminse brittle. Optic axial
angle 714°. G.c. : alumina 423, lime 15, potash 3'2, soda 69,
silica 41*6, water 5*5. Unionville in Pennsylvaniai
524. Clintonite, (|ft3 + j'Al)„gi + ja.
Oblique prismatic; in hexagonal tables, or massive foliated. Cl.
basal, perfect. H. — 5to5'5; G. — 3'15. Translucent ; pearly to
metallic on the cleavage. Angle of the optic axes 3 to 13°.
Reddish brown to yellow. C.c: 397 alumina, 21-1 magnesia, 13 '1
lime, 19 "2 silica, 2 protoxide of iron, 4"9 water. Amity and War-
wick in New York. Brandisitc is similar.
525. Xanthophyllite.
Oblique prismatic, C about 90°. Crystalline aggregates. Radiate
lamellar. H. — 4'6 to 6; G. — S'l. Lustre pearly. Colour yellowish
to copper-red. Angle of optic axes 0° to 20°. C.c: alumina 43 '6,
lime 13, magnesia 17'5, silica 16"9, water S'"* Zlatoust.
626. Chloritoid, FeSi-^A'lfi.
Right prismatic ; in foliated crystals ; brittle. Cl. basal.
Lustre greasy to pearly. H. =5'5 to 6 ; G. =3*52 to 3 '56. Dark
green; streak greenish white. C.c: 40 alumina, 27 protoxide ot
iron, 25 silica, 7 water. B.B. infusible, but becomes magnetic.
Decomposed by 3. acid. Hillswick in Shetland, Pregratten 111
Tyrol, Ekaterinburg, Canada.
527. Masonite.
Broad plates. H.=6*6; G. =353. Grey-green. Streak grey.
Pearly to vitreous. C.c: 26-4 alumina, 19 peroxide of iron, 16'7
frotoxide of iron. 32 '68 silica. 4 '6 water. Middletown in Rhode
sland.
528. Ottreute, AljSij + 3(Fe, Mn)Si-(-3fi.
Thin hexagonal tables Cl. parallel to the prismatic faces. H. —
5'5; G. — 4"4. Translucent; vitreous. Greenish or blackish grej.
C.c: 24'3 alnmina, 16'8 protoxide of iron, ll'l protoxide o£
manganese, 43'4 silica, 6'66 water. Ottrez in the Ardennes
(Luxemburg), Asto in the Pyrenees, Ebnat in Bavaria, Newport
(Rhode Island), Vardhos (Greece).
629. Pyrosmalite, 7feSi + RCl2-l-5a.
Hexagonal. P 101° 34'; crystals ooP, OP; tabular; also granular.
CL basal, perfect ; brittle. H. = 4 to 4-5 ; G. =3 to 3 2. Trans-
lucent to opaque ; resinous, or metallic-pearly. Liver-brown to
olive-green. C.c: 35 "5 silica, 37 "5 iron protoxide, 21 '6 manganese
protoxide, 8 chloride of iron or manganese, and 7 '5 water. Nord-
mark in Sweden.
530. ASTROPHYXLITE, (fu, ^)Si} .
Right prismatic, with oblique habit In long tabular prisms,
and in stellate groups. Cl.Das.al, perfect. H. — 35; G. =3'33.
Submetallic to pearly. Tombac-;brown to gold-yellow. Pellucid.
Axial divergence 118" to 124°. C.c. : peroxide of iron 9 3, protoxide
23 6, protoxide of manganese 10, soda 3-9, potash 6 9, titanic acid
7 "90, silica 39 '2. Brevig, El Paso in Colorado.
Chlorite Group.
531. Chlorite, 2ESi -^ ft^^l + 3S .
Hexagonal. P 106° 50'; crystals tabular of 0?, ooP or OP, P
(fig. 493) ; often in comb-like or other groups ;
generally foliated and scaly. H. = 1 tol"5; G. = 278 ^S i-^
to 2 -96. Leek-green to blackish green ; streak ^ 1^
greenish grey. C.c: 21 alumina, 20 protoxide j,. ^gg
of iron, magnesia 18, silica 24, water 11: Tarf- *'
side, Bute, and Jnra in Scotland. Cornwall, Cumberland, Wales,
Fassa Valley, Urals, America.
414
MINERALOGY
C32. rENNiNE, ^iiggi+fifgj'i^i+sa.
Hexagonal, rhoinbohedral ; R 65° 28'. Crystals chiefly very acute
rhombobedrons, with or without tho base. Lustre resinous. H. —
2 to 3; G. =2-6 to 277. Streak greenish white. B.B. exfoliates,
becomes white, and fuses on the edges to a white enamel. Com-
pletely sot. in warm s. acid. C.c: 83-6 silica, H'-I alumina,
?9 '4 magnesia, and 12-6 water; but with 5 to 6 iron protoxide re-
placing magnesia. Scalpa in Harris, Glen Lochy in Perthshire,
Zermatt in Valais, Tyrol, Ala di Stiira in Piedmont, MauMou
in the Pyrenees. LmchttnbcrgiU is the same. KiimmeTtrUe, with
5 to 8 chromium sesquioxide, is violet-blue or green ; Unst, Siberia,
Pennsylvania. ShodochTome and TabergUe are also varieties.
633. Clikocb-lore (llipidoUtc), 8ftgSi + lilg,,iij + 4a.
Oblique prismatic, C. 76° 4'. ooP 121° 28'. OP : P 118° 66';
OP : ooP 192° 8'. Crystals -2P, P, 4P»oo, OP {n, m, t, P, fig. 494).
Twins common ; lustre vitreous or resinous. H. =2
to 3; G. =2-6 to 28. B.B. becomes white, and
fuses on thin edges to a jgrcyish yellow enamel.
C.c: 30'3 silica, 17*8 alumina, 40'3 magnesia, and
12'1 water. Edentian and Blair Athole in Scotland,
Traversella in Piedmont, Akhmatovsk in Urals, West
Chester in Pennsylvania. CorundophylliU, Epi-
chlorite, and KotschtiitcyUe are varieties.
634. PVROSCLEEITB, (Jli, ife'jjSij+Sfi. Fig. 494.
Eight prismatic. CI. basal, perfect ; fracture uneven ; brittle ;
sectile. H.-3; G.=27to2-8. Pearly ; translucent. Apple-,
emerald-, and grey-green. C.c. : alumina 13-4, chrome oxide 1-4,
protoxide of iron 3 S, magnesia 31-6, silica 37, water 11. Porto-
Perraio in Elba, China.
533. Choniokiti.
Massive; crystalline-grannlar and ^lobolar-radiated. H. -2'6to
3 ; G. ■=2'91. Weak silky. White, with yellowish spots ; greenish
blue. C.c: 17'1 alumina, 22-6 magnesia, 12-6 lime, 35 '7 silica, 9
water. B.B. fuses easily, with intumescence, to a grey glass. De-
composed by h. acid, with separation of silica. Colmonell (Ayrshire),
Porto-Ferraio.
536. Ptcnotrop.
Large grained aggregates. CI. along two rectangnlar faces ; frac-
ture hackly, splintery. Greyish white to bromi-red. Vitreous to
greasy. H, =2 to 2-3 ; G. =2-6 to 27. Co.: alumina 29-3, mag-
nesia 12 6, potash 4 4, silica 46, water 7'8. Waldheim in Saxony.
537. Thcrinoitb. (i&, 63 + 4(4], fe))^^^* 4 rt.
Massive ; scaly. H. =2 to 2'5 ; G. = 3-2. Pearlv. Olive-green to
pistachio-green ; streak paler. Very tough. Powiler greasy. C.c:
alumina 16, peroxide of iron 14, protoxide of iron 33, silica 23,
water 11. Schmiedefeld in Thuringia, Harper's Ferry on the
Potomac, Hot Springs in Arkansas.
638. Delessite, (If'eJ, SlgljJij-ffilA, ¥oA)gi-l-3fi + 2lflga.
Massive ; scaly. H. =2 to 2-5 ; G. =.2-6 to 1-89. OlivS-greeu to
dark green, passing to dark brick-red ;
streak light green. C.c: alumina 16 '3,
protoxide of iron 12 "6, magnesia 21, silica
31 "5, water 15 '8. Common in igneous
roclts of Old Red Saadstone and Coal-
measure age in Scotland. Oberstein,
Zwickau, Lagrfeve near Mielin.
539. CKONSTEDTrnt, 5FeSi -I- (te, iig),
Si-hSa.
Rhombohedr.il; radiated columnar. In ,0 t. nvi-
tapering hexagons, and hemihedral (figs. ^>SAv5. (Sp.5d9.) Fig.495.
495,496). CI. basM, perfect; elastic. H. -2-5 ; G. = 3'3 to 8-6.
Vitreous. Coal-black and brownish black; streak dark olive-green.
C.c: protoxide of iron 39, peroxide of iron 29, silica 22, water 11.
Huel Maudlin in Cornwall, Przibram, Brazil iSidcroschisoltte).
Talc and Sebpektine Gropf.
640. Talo, J'lg:3i, + a.
Right prismatic (?) ; rarely found In six-sided or rhombic tables ;
generally massive, granular, or scaly. Rarely hbrous. CL basal,
perfect ; soft, sectiie, and flexible iuthiu plates. H. -=1 ; G. «=2'6
to 2'8. Transparent in thin plates, and optically binaxal; pearly
or resinous. Color.rless, but generally greenish or yellowish white
to apple- or olive-green . Feels very greasy. B. B. emits a bright
light, exfoliates, and hardens (H. —6), but is infusible ; with cobalt
solution becomes red. Not sol. in h. or s. acid before or after igni-
tion. C.c: 63'5 silica, 817 magnesia, and 4'8 water. Unst in
Shetland, green ; Cairnic in Aberdeenshire, brown ; Greiner in
Tyrol, Sala and Falun, the Pyrenees. Used as crayons, also for
forming crucibles and for porcelain.
SUatUe, — Massive. Grey, red, yellow, or green. Shetland,
Sutherland, Portsoy, and near Kirkcaldy, Scotland ; the lizard
Point, Cornwall ; Brian9on, WunsiedeL Savage nations cut tho
steatite into culinary utensils.
Fotetojie is a mixture of talc, chlorite, and other minerals.
641. PiCROPHTLL, 3RSi-l-2a.
Eight prismatic. H. -2'6 ; G.-376. Dark green. Foliated,
shining. C.c: magnesia 30 1, protoxide of iron 6 '9, silica 49 '8,
water 9 '8. Sala in Sweden.
642. Picrosmike, 2lilgSi-hS.
Eight prismatic, but massive. CI. cx>f no perfect, less so in other
directions ; sectile. H. = 2'5 to 3 ; G. =2'6 to 27; Translucent or
opaque ; vitreous, but pearly on oapoo . Greenish white, grey, or
blackish green ; streak colourless. Yields a bitter odour when
breathed on ; hence the name. C.c; 65 '8 silica, 36'1 magnesia, and
8*1 water. Presnitz in Bohemia, and Greiner iu TyroL
543. MoNRADITE, 4(|!ylg, JFe)Si + a.
Massive, foliated, translucent, and jrellowish-grey, H. ■■6 ; G. »
3'27. C.c. : silica 55 '2, magnesia 31 "9, protoxide of iron 8*8, water
4"1. B.B. infusible. Bergen in Norway.
644. Meerschaum, 2S[g2Si8 + 4B.
Fracture earthy ;. sectile. H. =2 to 2-5 ; G. -0'8 to 1 (when
moist nearly 2). Opaque, dull. Yellowish and greyish white; streak
slightly shining. Feels rather greasy, and adheres strongly to the
tongue. C.c: 54*2 silica, 24 7 magnesia, and from 9 to 21 7 water.
Negropont, Anatolia, near Madrid and Toledo, Moravia, Werm-
land,
645. Aphrodite, 4]iIgSi-Hll.
Soft and earthy. G. -2-21. Milk-white; opaque. C.c: 62-9
silica, 86'3 magnesia, 11'9 water. L&ngban 'Sweden), Elba.
646. Spadaite, l(IgjSij-H4a.
Massive; fracture splintery; sectile. H. ~2'5. Translucent;
resinous. Red, with white streak. C.c: 67 silica, 81'6 magnesin,
11 '4 water. Capo di Bove near Rome.
547. Gymnite.
Massive. H. -2 to S ; G. = 1'9 to 2-2. Translucent ; resinous.
Dull orange-yellow. C.c: 41 silica, 37 magnesia, 22 water. Tyrol,
Passau, Texas, Barehills near Baltimore. I\-ickcl GymniU has 29 of
nickel oxide, replacing the water. Unst, Texas, Pennsylvania,
548. Saponite, (f'e(JaJ'lg)sSi5 + (Al3Pe)Si-H3a.
Massive ; sectile, and very soft. H. = 1 -5 ; G. = 2 '2 to 2 '3. White,
orange-yellow, pale green, and reddish brown. Feels gi-easy ; does not
adhere to the tongue ; falls to pieces in water. C.c: silica 40*8,
alumina 7'5, ferric oxide 39, magnesia 20'6, water 227. Occur*
in all the above colours in the later igneous rocks of Scotland, com-
monly. Lizard Point and St Clear in Cornwall, and Dalecarlia iu
Sweden. Pimclite has 2 "8 oxide of nickel.
649. Serpentine, 2lig.Si + J'lgft, .
Crystallization uncertain ; pseudomorphic after oliviiie, ■ &c. ,
generally massive, and granular or fibrous ; fracture flat-con-
choidal, uneven, or splintery ; sectile, and slightly brittle.
H.=3to3'5; G. — 2'5to27. Translucent to opaque ; dull resin-
ous. Green, grey, yellow, red, or brown; often in spots, stripes,
or veins ; streak white, shining. Feels greasy, and does not adhere
to the tongue. In the closed tube yields water, and becomes black.
C.c: 43"5 silica, 43*5 magnesia, and 13 water ; but with 1 to 8 iron
protoxide, and also carbonic acid, bitumen, and chrome oxide.
Varieties are — (1) Noble Serpentine, brighter coloured, 16H;0,
and more translucent; (2) Picrolite, or fibrous (H. "3'5 to 4*6);
(3) Common, or compact; (4) ChrysotiU {Baltimonte, Md-axiic), in
fine asbestiform fibres, easily separated, with a metallic or silky
lustre (G.- 2 '21 9).
Common in Shetland, Urquliart, Portsoy, Ballantrae ; Lizard
Point in Cornwall ; Norway, Sweden, North America. Chrysotile
at Colafirth and Fetlar, Shetland, Portsoy, Towanreiff, in Scot-
land ; Reichenstein in Silesia, the Vosges Mountains, and North
America. Serpentine is often a product of decomposition, or pseudo*
morph of various minerals, as augitc, hornblende, olivine, spinel,
enstatite, garnet, kc. It forms wiolo rocks and mountains, and is
manufactured into various oniamenlal articles.
550. Marmolite, 31lgSi^-2Slga2-
Oblique prismatic; often foliated. H. — 2"5 to 8; 6. — 2'41 to
2"47. Lustre pearly. Greenish white, bluish white, and asitaragus*
green. C.c: silica 42*1, magnesia 38"6, water 17"5. In veins
in serpentine of Urquhart aud Portsoy (Scotland) Cornwall, Fin-
land, Hobokeu.
551. Antioorite.
Thin flat lamina!. H. -»2'5 ; G. -2'6. Translucent. Green with
brown spots ; streak white. C.c: silica 40'8, magnesia S6'3, f rot-
oxide of iron 6'8, water 124. Antigorio in Piedmont.
aii^EKALOGY
415
i52. Hydeophite, (Jig, fe)j§i,+4li.
Maasire and 6brous. H. —3 to 4 ; G. «2'65. Moantain-green to
blue-black,; streak paler. ■ C.c: silica 36 '2, magne8ia21'l, protoxide
of iron 227, water 16. Taberg in Sweden, New York.
653. TiCLAESITE, 2ilg2S' + S.
Right prismatic ; crystals P, OP, meeting at 138*32', often twins
in tnple combination; also granular. H. — 3 ; G. ■=*2'9 to 3. Trans-
lucent. Greenish to greyish yellow. C.c: silica 39'6, magnesia
47 "4, protoxide of iron 3-6, water 6 '8. Totaig, Boss-shire ; Tiaver'-
sella. Piedmont ; Forez, France.
S54. Pykju-lolite.
Oblique prismatic, C 72° 5S' ; columnar and grannlar. CI.
basic and hemidomatic, meeting at 94° 36' ; fracture splintery ;
brittle. H. — 3'5 to 4 ; G. — 2'fi. Translucent on edges ; resinous.
Greenish to yellow-grey. Cc: silicate of magnesia and water.
Storgard in Finland.
655. Deematine, (Sig, fe)Si-f2fi.
Reniform ; stalactitic; fracture conchoidal ; brittle. H. =2*5;
G. -=2'1. Resinous. Blackish green ; streak yellow. Does not
adhere to tongue. C.c: silica 38, magnesia 22, protoxide of iron
12, water 23. Waldheim in Saxony.
656. Chlorophsite, ftSWB,Si3-h4S.
Massive, rarely reniform. Coating or filling up geodes in amyg*
daloidal cavities. H. -1-5 ; G.- 2 02 to 2 3. SectUe ; fracture con-
choidal. On firat exposure transparent and oUve-gr^en to orange-
yollow, but soon changes to black and opaque, splitting in so
joing. Titreous to shining. B.B. melts to a black glass. C.c:
silica 36*2, alumina 8 '9, peroxide of iron 13 '8, protoxide of iron
2"4, lime 3 "8, magnesia 10, water 24*8. Rum and Canna in the
Hebrides, Giant's Causeway. The original mineral from Rum has
22*8 iron peroxide and no alumina.
857. FORCHHAIIMERITE, f'eSi -H 6S .
Granular massive. Subresinous to dull. Dark green. H. =2;
G. = l*8. C.c: silica 32*8, protoxide of iron 21*6, magnesia 3*4,
water 42*2. Faroes.
658. KiRWASITE.
Fills druses in amygdaloids with divergent sheaf-like crystals.
H. =2;G. — 2*9. Opaque. Olive-green to dark green. C.c: silica
405, alumina 111, protoxide of iron 23*9, lime 19*8, water 4*4.
Locli Baa in Mull ; Moutne Mountains in Ireland.
659. Gladcosite.
Round grains. Dull resinous. Light green. C.c: silicate of
protoxide of ii-on and potash. Ashgrove near Elgin ; greensand
of England, France, Germany, and Ajonerica.
660. Celadonite, 3ftSiJ-^83Si2-^5rt.
Massive, forming crusts, as of agates. Earthy, sectile, H. = 1
to 2; G. -2*6 to 2*8. Opaque, shining. Bright gieen. Feels
(»reasy. C.c: silica 54, alumina 3 8, ferric oxide 11*9, ferrous oxide
5*4, magnesia 6 8, potash 7*9, water 10. Orkney, Rum, and
Fircshinj in Scotland. Giant's Causeway, Verona, Faroes, Iceland,
Cyprus, Bohemia.
561. Stilpxomelane, 2(Pe, Jlg)Si -(■ MSi -f 23 .
Jtassive or radiating-foliated. One cl. perfect ; brittle. H. = 3to
4;G.— 3to3*4. Opaque ; vitreous topearly. Greenish black. C.c:
45 -3 silica, 6*9 alumina, 38*3 iron protoxide (with 2 to 3 magnesia),
and 9*5 water. Zuckmantel in Silesia and 'VVeilburg in Nassau.
662. CUAMOISITE.
Oolitic and massive. H. - 3 ; G. - 3 to 3*4. Greenish grey to
black; streak paler. C.c: silica 14*3, alumina 7*8, protoxide of
iron 60*5, w.atcr 17*4. Chamoison (or Chamoson) in Valais, the
Vosges. Bcvthicriiu: has 75 (irotoxide of iron and 5 of water ;
Moselle.
AtrorrE and Hokkblende Group.'
Hornblende and augite rather represent groups of mineral sub-
stances than single species. They are best distinguished when
imperfectly foimed, by the cleavage and angles of the prisms.
663. E.\*sTATrrE (ChlndnUe), SlgSi .
, lUffcr too wldclv to jiistify their anion, Homblende la more fusible,
and ranees lower In Bpcclfic gravity (homblende from 2-931 to 8-445, aoKlto
3-195 to 3-525). lliough boTh posscsa s clearage parallel to their vertical
prisms, yet these differ In angular dimensions :— hornblende 124* 12', ougite 87*
6*. They also occur indistinct geognostic positions; — hornblende in rocl^s con-
taining quartz or freo silica, and mostly Vfitll minerals that arc neuti-al compoantJa
of silica, as orlhoclase and atblte ; augite in rocks that do not contain free silica,
and mostly with minerals that are not neutral silicates, as labradoilte, olivine, and
leucite. Hence there arc two distinct series of massive or igneous roclts : — the
hornblende series, including grsnlte, syenite, dlorlte, dioritc-porphyry. and red
porphyry ; and the augite series or hypcrsthese rock, gabbro, dolerlte, nepbellae
roca, au^ito-porpbyry, and Icucltc-potpbyry.
Right prismatic ooP 92° to 98°; crystals ooP<o (o),
ooP (m), JP.O (i), jI'M (9),
Jpco (+), iP (t) (fig. 497).
Usually imbedded, or indis-
tinct granular masses. Cl.
macrodiagonal very perfect,
Srismatic ooPdistinct, brachy-
iagonal imperfect. H. = 5*5;
G. -31 to 3-3. Translucent
throughout, or only on the
edges ; vitreous or pearly on
the more perfect cleavage-
planes. Colourless, greyish
or greenish white, yellowish,
or brown. Not affected by
acids. B.B. almost infusible. Fig. 497.
C.c: 60 silica and 40 magnesia, but with 6 to 8 iron protoxide,
1 to 2 alumina, and 1 or 2 water. In olivine and serpentine
ro^ks in Moravia, the Harz (Baste), and the Pyrenees.
564. Bronzite {SchilUr Spar, Saslik), (Mg, te)Si.
Bight prismatic ooP 94° ; only granular and foliated. Cl.
brachydiagonal perfect, prismatic less so ; fracture uneven, splin-
tery. H. -4 to 5; G. -3 to 3*5. Translucent on thin edges;
metallic pearly. Green, inclining to yellow or brown. Imper-
fectly soL in h. acid, wholly in s, acid. B.B. becomes magnetic,
and fuses in very thin splinters. C.c: 43 silica, 26 magnesia, 2*7
lime, 7*4 iron protoxide, 3*3 iron peroxide, 2*4 chrome oxide, 1*7
alumina, and 12*4 water. BaHitc is possibly altered enstatite.
Belhelvio and Black Dog in Aberdeenshire, Baste, Tyrol, Baireuth,
Styria.
565. PAtTLITE {Hyperstheiw), (Fe, J'lg)Si.
Right prismatic ooP (m) 93° 30', P2 (c), 2P2 (0, iH («)>
oop2 (n), iP«> (A), ooPoo (a), oofoo (6), Jpoo (i), 2Poo (rf).
Granular or disseminated. CL brachydiagonal very perfect,
prismatic ooP distinct, macrodiagonal very imperfect. H. = 6 ;
6. —3*3 to 3*4. Opaque or translucent on thin edges ; vitreous or
resinous, but metallic pearly on the cleavage planes, of which one is
■^p^s^ copper-coloured to violet or silvery. Pitch-
black and greyish black ; stieak greenish grey
or pinchbeck-'brown, inclining to copper-reti
Not affected by aoids. B.B. melts more or
Fig. 498. Fig. 499.
less easily to a greenish black glass. Often magnetic C.c : gene-
rally 46 to 58 silica, 0 to 4 alumina, 11 to "JS magnesia, 1 to 5
lime, 13 to 34 iron protoxide, 0 to 6 manganese protoxide. Portsoy
and Craig Buroch in Banffshire, Bana Hill in Aberdeenshire, Paul's
Island, Labrador, and Greenland. Crystals occur in eauadine
bombs at Lake Laach {AmUysttgiU), and in meteorites of Breiten-
bach. Hypeisthene rock in Norway, Elfdal in Sweden, Cornwall
(!), the Harz, and Canada. Chemically enstatite and paulite pass
into one another ; the essential difference is that the axial dispersion
is uniformly (><i/ in the former, and the opposite in the latter.
566. WOLLASTONiTE(TaJi<?ar 5^o)), CaSi.
Oblique prismatic, C 84° 30'. ooP 87° 18', OP (« or *'),
ooP« (c 01 p), ooPJ (2) 110° 7',
ooP'2(xor<051°, -Peo (»)44°
27', ^Poo (o) 69° 56' (fig. 600).
Rarely crystallized, mostly
broad prismatic or laminar.
Frequently fibrous. Cl. along
OP and e»P°oo perfect, but
planes uneven or rough ; meet
at 95° 23'. H. - 4 -5 to 5 ;
G. - 2 -8 to 2 9. Translucent ;
vitreous or pearly on cleavage.
White, iucliniiig to grey, yellow, red, or brown ; streak vhite.
Fig. SCO.
416
MINERALOGY
Phosphoresce with heat or friction ; gelatinizes in h. acid. B.B.
difficultly fosibio to a scniitninsparciit glass. C.c: 51-7 silica
and 48 '3 lime, but with 0
to 2 magnesia and 0 to 2
iron protoxide. Glen Gaim,
Crathie, ice, in Aberdeen-
shire, Urquhart in Inver-
ness, Skye, Banat, Finland,
Sweden, Vesuvius (fig. 501),
North America, Ceylon, Capo
di Bove.
56/. AuoiTK (Pyroxene),
KSi-(Ca, %, fe)Si.
Obliqueprismatic, C 74*11'.
ooP87^6'^; P(i:s)120°4S';
-P(t0131°30'; 2P(o)95°
Fig. 501 (sp. 566).
4S'; OP; 3P ; ocPoco. In fig. 130 o=P (J/), ooP^oj (r), o>P«a>
(OfP(s): also various twins and hemitropes of same form (figs.
191, 502, 503). Almost alwaj-s prismatic, imbedded, or attached ;
ako granular, columnar, and scaly. CL prismatic along oaP (with
Fig- 502. "*' Fig. 503.
angles of 87° 6' and 92° 54'X generally rather imperfect ; ortho-
diagonal and clinodiagonal imperfect. H. = 5 to 6 ; G. - 3 to 3 5.
PeUncid in all degrees; vitreous; in some pearly on 06P°<o. Colour-
less, and white, but usually grey, green, or black B. B. generally
fusible; imperfectly soluble in a'cids. C.c. generallyas follows
|smc».|Lime.
Magnesia.
Iron.
ic
25 M
23-81
16-24
8-50
14-97
2S-e5
(6) Magnesia-iron
(e) IroQ Bugite —
aufiite
.../. 52-72
Analysis gives 47 to 56 silica, 20 to 25 lime, 5 to 16 magnesia,
1 to 20 iron protoxide, with 0 to 3 manganese protoxide and 0 to 8
alumina. The alumina, chiefly found in very dark green or black
angites, may in some replace either silica or part of the silicate.
The more important varieties are-^
Piopsitk.—Gttyish or greenish white, to pearl-grey or leek-green;
streak white. Crystallized or broad columnar, or concentric
Iamell.ir. Transparent to translucent on the edges. Xot afi'ected
by acids. B.B. fuses to a whitish semitransparent glass. C.c:
generiUy lime 26 and magnesia 185, with 55-5 silica, llussa Alp
(iliLssUe) and Ala {Alalitc) in Piedmont, Schwarzenstein in Tyrol,
Scandinavia, Finland, Urals, and Xorth America.
MalacolUe, Snhlite.—\\'\ale, green, rarely yellow, brown or red;
streak white. Translucent, or only on
the edges ; vitreous, inclining to pearly.
Seldom crystallized, mostly columnar
Fis. 505.
§f^-
Fij. 504.
or lamellar. B.B. melu to a dark-
coloured glass. Malacolite common in
primary Uuiestoncs in Scotland, as at
Shinuess, Ledbe" (fig. 505), and Glea
Fig. 606.
oninuess, L«:aDe<! (ng. sua), and tilea ng. wo.
Tilt Fasia Valley i^FataaiU), Kcdjaont. .Vrcadal, Philijutaut in
Sweden; LaV.e Baikal (BaiJaiUU): near Lake Ll>5r2 in the Pyrenees
(.Lhtr^olilr.) ; Sila (or Sahla) in Sweden (Sahlitt) ; Shinness (figs.
504, 500), Gleaelg, Tirce, in Scotland ; Tyrol ; North America.
CoccoliU is a granular sahlite or angite.
AugiU. — I^k-green. greenish olack, or velvet-black, r»rsly
brown ; streak greenish grey. Vitreous to resinous ; translucent
or opaque. Only slightly affected by acids. B. B. fuses to a black,
often magnetic 'glass. An essential component of many rocks,
as basalt, dolerite, clinkstone, and augite porphyry ; Germany,
Auvergne, Vesuvius; St Hilda, Bum, Tiree, Dalnain, and Urqnh.irt
in Scotland. Augite crj'stals in basalt often contain very many mi-
croscopic crj'stals and glasses ; also pores with fluid carbonic acid.
SudsoniU. — Cleavable lamellar, and jet-black, with green streak
and bronzy tarnish, from the Hudson river ; the most mghly ferru-
ginous variety.
Amiaiilhus. — Some osbestiform minerals are augite, but the
greater number hornblende.
BreislackiU. — Fine yellowish or brown woolly crystals. Vesuvius,
and Capo di Bove near Bome.
568. DuxLAOE, (Ca, Mg, fe)Si.
Like angite, and only a variety with very perfect cleavage in
the clinodiagonal, wliich forms with a second cleavage an angle of
87°. Lustre metallic pearly ; colour grey or pinchbeck-brown.
H. -4; G. =3-23. B.B. melts easily to a grejish or greenish
enamel. C.c.: 50 to 53 silica, 1 to 5 alumina, 35 to 23 magnesirs
11 to 20 lime, and 5 to 20 manganese protoxide. Constituent of
the augite rock of the Cuchullins in Skye and of the gabbro of L'nst
and Ayrshire. Baste in -the Harz, Silesia, the Alps, Apennin'^
and Urals. VanadiTU-BronziU, containing soda and vanadic scij^
is similar. At Craig Buroch (Banff"shire) diallagc passes in paulite.
569. Jeffeesoxite.
Oblique prismatic. CI. prismatic ooP 87° 30', and orthodiagonaL
H. = 4*5; G.™ 3 "3 to 3 •5. Dark olive-green, brown to black. Lustre
greasy. A manganese and zinc angite, ^\-ith 10-2 protoxide of
manganese, and 10'15 oxide of zinc. Sparta in New Jersey.
570. AcMFTE, 2FeSi,-l-3RSi.
Oblique prismatic. Crystals long often acute-pointed prisms.
O.P 87° 15', o=P<o (r), P(5), 6P (t), - 6P'3(c) (figs. 507, 508). CL
like augite. H. =6 to 6 '5;
G.=3-4 to 3-6. Nearly
opaque; vitreous. Brownish
or greenish black ; streak
greenish grey. Imperfectly
soluble in acids. B.B. fuses
easily to a black magnetic
glass. C. c. : 52 silica, 30 iron
peroxide, 5 iron protoxide,
and 13 soda, but with 1 to 3
manganese jieroxide, and also
3 to 4 titanic acid. Eger and
Porsgrund in Norway.
571. .£c£KiXE,K^"i5-H'8Si
-h2SfaSi.
Oblique prismatic; striated f"'S- 507- (Sp. 570.) Fig. 508.
or reed-like prisms of 66° 30' to 87' 45'. C\. orthodiagonal per-
fect, less distinct clinodiagonal, and prismatic. H. — 6'5 to 6;
G. -3-4 to 3-5 or 36. Vitreous; translucent on edges, or opaque.'
Greenish black. B.B. fuses easily, colouring the flame yellow.
Scarcely affected by acids. C.c:' 49 silica, 317 iron peroxide,
6-6 iron (and manganese) protoxide, and 127 soda, with a little
magnesia and rwtash. Has the same relation to angite as arfved-
sonite to hornblende. Near Brevig and Barkevig in Norway.
572. Spoduuene, 4i'li'i,-(-3(ti, Sr,n, ]t)Si.
Oblimie prismatic, C 69° 40'. ooP S7° (fig. 509). CI. prismatic 0.P
and ortliodiogonal, perfect; chiefly m.issive
or foliated. H. «.6o to 7; G. -31 to
32. Translucent ; vitreous or i)early.
Pale greenish grey or white to appl'e-
green; streak white. B.B. intumesces
slightly, tinging the flame momenurilv
purphsh red, and fuses easily to a colour-
less glass. Not afl'cctcd by acids, C.c:
65 silica, 2S7 alumin.i, and 6-3 lithia.
Killincy near Dublin, Uto in Sweden
T>-rol. KilUniu (sp. 651), from Killiney,
seems to be decomposed spodumcne.
573. Petaute ICastor), 4'AlSi,'^S;t!,
lJa)Si,.
Oblionc prismatic Castor has C 67°
34' and ooP 86° 20', in irregular rect-
angular prisms, potalite being massive Pig- 509 (sp. 572).
and coarse granular. CL basal, distinct; in a second directioa
MINERALOGY
417
Fig. 511.
(meeting at 141i°) less so. H. -6-5; G. -2-4to 25. Greenisn,
greyish, or reddish vthite to pale red. Translucent ; vitreous or
pearly. B.B. melts easily into a porous obscure glass, colouring
the flame red. Not affected by acids. C.c. : 78'3 silica, 17'4 alu-
mina, 3 2 lithia, and 11 soda. TTto, Bolton in Massachusetts,
Yorls in Canada. Castor in Elba, itilarite, valley of Hilar,
Switzerland.
574. RnoDONiTE (Manganc$e-Spar), JlnSi .
.Vnorthic. ooP«>(a); »P«o (J); OP (c): »?'{«); f'oo (t-); Poo(j);
'poo (o);m'P'«. ((): a: 6 111" 9'; c: o93°28';n: o 106° 19'; but
chiefly massive or granular.
CI. (»Poo and OP, meeting
at 87° 38', perfect ; brittle.
H. = 5 to 5-5; 0.-35 to
3*7. Tmnslucent ; vitreous
or partly pearly. Dark
rose-red, bluish red, or red-
dish brown. Not affected
by acids. B.B. fusible.
C.c: 45-8 silica and 54-2
manganese protoxide, with ^^*
3 to 5 lime and 0 to 6 iron protoxide. St Marcel, Likngbani
Ekaterinburg, the Harz, and New Jersey. BustamiU, pale
greenish or reddish groy, with 14 lime, Mexico ; FcrwleriU^ New
Jersey, with 7 to 11 iron protoxide; and PaisbergiU, Sweden, are
varieties. Hydropite, Pkoticiief AUaffite, and Horn-Manganese
are mere mixtures.
575. B.4.BINGT0NITE, 9{Ca, i'e, I'injSi-l-FeSij.
Anorthic. Crystals very low eight-sided prisms, small, attached,
ff : A 90° 24' ; c : a 87° 27' ; o : (> 112°
12' ; b:d 81° 8' ; c : d 150° 10' (fig.
611). CI. basal (c), very perfect; also
along b. H.-5-5 to 6; G. = 3-3 to
3*4. Thin laminre translucent. Splen-
dent vitreous ; black. Not affected by
acids. B.B.. fuses easily wiih efferves-
cence to a black magnetic bead. ^.c. ;
50"7 silica, 11 iron peroxide, 10'3 iron
protoxide, 77 manganese protoxide,
and 20-3 lime, in the Arendal speci-
mens ; one from Nassau gave about
17 of peroxide, with protoxides only 11. Tongue (Sutherland),
Portsoy (Banffshire), Arendal, Nassau, and Gouverneur (New
York).
676. SzABorrE, ll¥eSi3 + 2CaSi.
Anorthic. o<>P'(;); oo'P (m) 88° 40' ; ooPw (J); oopoo (o) ; F(p);
*P (o); 2'F,<x> (y) ; 2p'oo (x) (fig. 512). H. =
6 "6 ; G. = 3 "5. Brownish red to reddish
yellow. Pleoehroic C.c. : silica 52 '4, per-
oxide of iron 44 7, lime 3 1. Slightly sol.
in 8. acid, more so in h. acid. Calvario on
Etna, Mont Dore.
577. AXTHOPHYLLITE, 3l'lgSi -I- FcSi . "'
Eight prismatic. ooP 124° 30'. CI.
macrodiagonal, perfect. Clove-brown to
fiurplish brown and leek-green. Trans-
ucent; radiating and folinted. Pearly on
cl. plane. H. = 5-5 ; G. =3-2. C.c. : silica
55 '9, protoxide of iron 167, magnesia 27 8.
fusible. Hillswick, Shetland ; Kongsberg and Modum, Norway";
Greenland, and the United States.
578. HORXDLEXDE.
Oblique prismatic (figs. 513 to 517; seo also 6g. 192). Distinct
cleavage in several direc:ions. H. = 4 to 6, but generally 5 (will
scratch with knife); G. -2-5to 4 0, but mostly high. Mostly
coloured. Lustre vitreous, in some silky or metallic pearly. Sol.,
but not very re.idily, in acids; more or less easily fusible. C.c:
anhydrous silicates and aluminates of lime, magnesia, iron pro-
toxide; moro sparingly of soda, yttria, and manganese protoxide.
Tho chief species form by their decomposition highly fertile
soils.
./4m;)/ii4o?(;.— Oblique prismatic, C 75° 10'. ooP 124° 30', P
148° 30'. The crystals short and thick, or loug and thin prismatic ;
formed, especially by ooP (,„), ooP«« (x), and bounded on the
ends chiefly by OP (;,) and P (,). Twins common, with the
chief axis the twin axis. Very ofteu radiated, fibrous, or columnar,
"LJ?-"" ■, ^h prismatic along ooP 124i°, very perfect;
ortfcdlagoiial and clinoUiagonal very imperfea. H.=5 to 6;
lr.-.!9 to 3-4. Pellucid in all degrees ; vitreous, but sometimes
pearly or silky. Colourless or white, but usually some shade of Krey,
yellow, green, brown, or black. B.B. fuses, generally iutumescin-
aad boiling, to a grey, green, or black glass. Those containing
■f^
Fig. 512 (sp. 576).
B.B. very difficultly
most iron are most fusible, and are also partially soL in n. acid,
which scarcely affects the others. C.c very variable.; the silica
is partly replaced by alumina, specially in the green or black
varieties; KO is chiefly MgO, CaO, and FeO. Lime is the most
c Ig. 513. Fig. 514.
constant element, in most from 10tol2;magnesia and iron protoxide
replace each other, the one increasing as the other diminishes.
With 4Si and ft — 2Mg-HCa-Hfe, the average composition is 63 '6
silica, 17'8 magnesia, 12'5 lime, and 16'1 iron protoxide; bat
Fig. 515. Fig. 516. Fig. 517.
analyses give 40 to 60 silica, 0 to 17 alumina, 0 to 30 magnesia,
10 to 15 lime, 0 to 36 iron protcxide (or peroxide), and 0 to 4
manganese protoxide, 0 to 8 soda, 0 to 3 potash, and 0 to 15
fluorine with a little water.
The more important varieties are —
Amianlhzis, Asbestos, ini BtjssoliU, 2ilgSi -H CaSi . Fine fibrous.
White, grey, or green. The fibres ,often easily separable, elastic,
and flexible. Unst, Shinness, Portsoy, Savoy, Tyrol, Corsica,
TrcmoHte, Grammaiite, SltgSi -^ CaSi, with 68 '35 silica, 28 •Sg
magnesia, and 13 "26 lime. Wiiite, grey, green ; in long prismatic
crystals, often striated longitudinally. Pearly or silky ; semi-
transparent or translucent. B.B. fuses readily to a white or nearly
colourless glass. Loch Shin (Sutherland), Glen Tilt, Gleneig,
Tiree, Cornwall, Cumberland, Sweden, the Alps, Pyrenees, Silesia,
Siberia, North America.
Nephrite, or Jade, is a tough, compact, fine-grained tremolite, with
H. — 6 to 6'5 ; G =29 to 31. Fracture close splintery. Very
tenacious. Translucent ; dull to resinous. Leek-green to blackish
green. Feels slightly greasy. Formerly made into ring-stones,
amulets, idols, and war axes. New Zealand^ China, Mexico, Peru,
BalU (Shetland).
ActinoUle, Aclinote, or Slrahlstiin (Ca, Jig, f e) Si . Colour
green, inclining to black, grey, or brown. Translucent througii-
out, or only on the edges. Long prismatic crystals, or radiated-
columnar. masses. B.B. melts to a greenish or blackish enamel.
Fethaland and Colafirth and Hillswick (Shetland), Oronsay, Ord
Ban (Inverness), Sweden, Tyrol, North America.
EornbUnde. — eRSi-fSjSij. Green or black, seldomer brown or
grey. G. -31 to 3-3. B.B. fuses rather easily to a yellow,
greenish, or black enamel. Three varieties are distinguished, (a)
The noble or Pargasil^, pale celadon- or olive-green, and strojt;^
pearly or vitreous lustre ; at Pargas in Finland, Tyrie in Scotland.
(6) Common hornblende, dark leek- or blackish-green, opaque ;
streak greenish grev. A constituent of many rocks, as in Norway,
the Alps, and Scottish Highlands (Ballater, Ben Arihaar, Glen-
bucket, Colafirth). (e) Basaltic, foliated, with bright even cleavag.-,
opaque, velvet-black ; streak grey or brown. Generally contains
alumina (9 to 15) and much (5 to 11) iron peroxide. In basalt and
volcanic rocks: Etna, Vesuvius, Rhineland, Bohemia.
XVL — Si
418
MINERALOGY
579. ARrrEDsoNiTE, KSi +$ebi5 .
Obliquo prismatic. ocP; ooP^m ; P; 2P°oo 120° 24'; OP. CL ooP
124° 22', perfect; also OP. Maesive. Black; opaque. Vitreous.
H. — 6; G. — 3'44. C.c. : silica 43, alumina 45, peroxide of irou
3-8, proto.tido 34, limo 57, soja 8'5. Streak dark blue-grey.
Fusible in fine splinters in the flame of a caudle. B.B. intu-
mesces and melts easily to a black magnetic globule. Not sol.
in acids. Kangerdluarsuk in Greenland, Frederiksvarn, Arcndal,
El Paso in Colorado.
680. PiLOUTE, 4J"IgSi,+':^rSi; + 15S.
Felted or matted fibres moro or less dense. Cream yellow to
buff. Dull ; extremely tougb ; absorbs water like a sponge.
H. - 1 to 2-5 ; G. - -68 to 1 -34. Structure varies considerably, aud
has given rise to trivial names, as mountain paper, mountain
leather, mountain flesh, rock cork, kc. MomUavi I'apcr occurs in
thin sheets at Boyna Castle near Banff ; Mountain Ltather, Burn
of the Cairn (Cabracli), Tod Head (Kincardineshire), Leadhills,
Strontian ; Sock Cork, Portsoy aud Boyno Castle, Saxony, and
Sweden. C.c. : silica 51'6, alumina 86, ferrous oxide 2S8,
magnesia 10"2, water 23 "3.
581. Krokidolite, 3FeSi + (Sa, Mg)Si. + 2fi .
Delicate, easily separable, but tou"h fibres ; elastic H. = 4 ;
G. =3'2 to 3 '3. Translucent ; silky, fndigo-blue ; streak lavender.
B.B. fuses easily to a black magnetic glass. C.c: silica 50*3, iron
protoxide 35, magnesia 2 '2, soda 67, water 5 '8. Stavern in
Norway, Gi-eenland. A iibrous yellow mineral from Orange river.
South Africa, has been referred here ; its fibres are not separable,
and its hardness is 7. AbriachaniU. a very similar mineral, of blue
colour, occurs near Inverness.
582. Glaucopha>.-e, 91tSi + 2*1313 .
Oblique prismatic. CI. prismatic, perfect ; fracture conchoidal.
H. — 6'S; G. — S'l. Translucent; vitreous to pearly. Indigo-
blue, grey, bluish black. B.B. becomes brown, fusing easily to
olive-green glass. Co.: silica 56 '5, alumina 12*2. protoxide of
iron 10-9, magnesia 8, soda 9-3. Island of Syra.
583. HcnM.^NN-iTE, j'lnSi .
Granular aud arborescent. Rose-red. G. = 3-4. C. c. : protoxide
of manganese 46 7, silica 48 "9, lime 2, maguesia 2*4. Cummiugton
in Massachusetts.
5S4. GiiusEKiTE, FeSi.
Asbestiform. G. — 37. Brown ; silky lustre. C.c. : protoxide of
iron 51-55, silica 45-45. Mt. dcs Manres (Var).
535. loLITE {Cordicrite, Z)ic/iroi(«), A^Sij-H 2(Mg, Fe)Si.
Right prismatic. ooP {P) 119" 10', middle edge of P 95° 36'.
Form ooP (T), oofoo {I), OP (m) ; and this with mPm (i),
ooP3 (rf), P» («)> and JP (j), (fig. 518); short, prismatic CI.
ooPoo distinct, traces along Pm ; fi-acture conchoidal or uneven.
H. -7 to 7-5; G. -2-5 to 27. Trans-
parent or translucent ; vitreous, inclining
to resinous. Colourless, but chiefly dark
hlue, or violet, green, brown, yellow, and
grey. Often with distinct trichroism ; on
OP blue, on o-Poo grey, and on oopto yel-
lowish. B.B. fuses difficultly to a clear
^lass ; slightly affected by acids. C.c. : 48
to 51 silica, 29 to 33 alumioa, 8 to 13 mag-
nesia, 1 to 12 iron protoxide. Cabo do Gata
in Spain, Bodenmais !,PcUom), Orijerfvi in
Finland ISIcnJuilitc), Norway, Sweden,
Orcenland, North America, aud Siberia.
Small rolled masses of an intense blue colour
and transparent, found in Ceylon, are the
Sapphire (CSnu or Luch$$apphir of the jewellera.
The following have been considered cortlierite altered, or with 2 to
-6 atoms water: — (rt) BoJisdorJilc, Hydrous foiiU, greenish brown or
dark olivo-green ; near Abo. (4) JSsmnrkUe, Clihrophyllile, large
prisms or foliated, gi-con or brownish ; near Cabrach (Aberdeen),
Brerig in Norway, Unity in Blaine, and Hivldam in Connecticut
\c) F^UimiU^ TriclasiU, com pact, greenish bi-own or bhick, foliated ;
H.-2-5 to 3; 0.-25 to 28; Falun, (d) Huronilc, granular;
pearly, yellowish-grcon ; H — 3-3; G. — 2-86; infusible and insol-
uble ; Lake Huron, (t) JFcissiU, kidney-shaped and ash-grey or
brown ; Falun and Lower Canada. (/) PyrarjilliU, indistinct
imbedded crystals, black passing into brown or red, dull resinous
lustre; H. -36; G. -2 5; Hclsingfors. (?) PiniU, crysUUired,
or missive and laminar, with imperfect cleavage; H. — 2 to 3;
<3. -27 to 2-9, scmitranslucont or op.aquo, dull or resinous, and
dirty grey, green, or brown ; B. B. fuses to a ghiss, sometimes clear,
at other timas dark-coloured ; Auvei-gne, Schneeberg, Pcni^ in
Saxony, the Harz, Cornwall, C&bracU and Xorry (Aberdseouin),
Fig. 518.
the United States, and Greenland (Oitxddte, %f. 650). OosiU from
GeroldsAU in Baden, snow-white, opaque, fragile, is similar. (A)
QigantoliU ; H. — S'S ; G. — 2 8 to 2 9; opaque, dull resinous, and
greenish grey or brown ; B. B. intumesces slightly, and fuses easily
to a greenish slag ; Tanimela in Finland. (i) PrascoliU lamellar
and green; Brevig in Norway.
586. Emerald (Beryl), 'i^lSi, -h SGlSi .
Hexagonal ; P 69° 53'. Crystals of c»P, OP, and o»P, ooP2, OP," P
(n, p, d, s, fig. 519) are prismatic,
generally with vertical atriie. CI.
basal, rather perfect; ooP im-
perfect. H.- 7 -6 to 8; 0.-26
to 2 8. Transparent or trans-
lucent ; vitreous. Colourless or
white, but generally green, some-
times very brilli.-.nt; also yellow
and smalt-blue. B.B. melts with
difl[iculty on the edges to an obscure
vesicular glass. Not affected by
acids. C.c: 67 5 silica, 18-7
alumina, and 13-8 glucina, with
0 3 to 3 iron peroxide, and 0 3
to 3-5 chrome oxide in the rich
green emerald. Ejncrald, bright
green ; G. -2710 to 2-769; occurs
in Muso Valley near Bogota, also *^K- ^l^-
in Salzburg and the Urals. BerrjJ, or Aquarnari^u, colourless, or
less brilliant; G. -2677 to 2-725 ; near JIursinsk and Ncrtcllinsk
in Siberia, Salzburg, and Brazil ; in the United States, where at
Grafton, between the Connecticut and Merrimack, crystals 4 to 6
feet louw, and weighing 2000 to 3000 lb, occur : Mourne Moun-
tains in Ireland ; Mount Battock and Cairngorm in Scotland (fig.
98). Common Beryl at Falun in Sweden, Fossum in Norway,
Limoges in France, Rabenstein in Bavaria, Nigg Bay and Pitfodels
and Rubislaw near Aberdeen {Daridsonite), Struay Bridge (Ross),
Emerald and beryl are much valued as precious stones. Known
from quartz by face p. Forms shown in figs. 92, 95, 96, 97, 98, 276.
687. Leucophane, 6CiiSi-f 3Giei + 2NaF.
Right prismatif. ooP 91°. CI. basal perfect. H. -3-5 to 4;
G. — 2-97. Pellucid. -Wine-yellow to olive-green. Vitreous.
B.B. fuses to i>ale violet-blue bend. C.c: silica 47, lime 23'4,
glucinalO-7, soda 113, fluorine 6-6. Lamo in Norway.
588. Melinophake, 7(k3Si;)-h6NaF.
Pymmidal. P 122° 23'. 'Mostly lamellar.' H."- 5 ; G.=|.
Honey -yellow to citron-yellow. Brevig and Frederiksviirn. •
Felspae GRorp.
Crystallization oblique prismatic or anoi-thic ; vei-y similar both
in aspect and in angles. CI. very distinct, especially the basal P;
less so the clino- or brachydiagonal JI. G. = 2-4 to 32, but mostly
2-5 to 2-8; H. -6or a little more. Slightly or not .at all soluble in
acids. B.B. fusible, but often with dirticulty. Ti-anslucent; pure
varieties transparent Colourless, white, or shades of red ; less
commonly of green or yellow. C.c: anhydrous silicates of alumina,
and of an alkali or alkaline earth. \
The felspars are very important constituents of the earth's crust,
occurring in nearly all the igneous rocks, and in many of tho
stratified crystalline schists. In true strata they arc found chiefly
as fragments or decomposed, and in tho latter state form a large
part of wet soils and clays. By tho older mineralogists and iu
popular language many s|>ecies are conjoined under the common
name of felspar which are now considered as distinct, each of tlieni
having not only its peculiar physical and chemical characters, but
also gcognostic position and associated groujis of minerals. Thus
orthoclase, and the other more siliceous felsi>ars w-ith potash, abound
iu granite and the plutonic rocks ; the less siliceous, with soda and
lime, characterize the volcanic rocks, — e.7., labradorite the basaltic
group, glassy felspar the trachytic Orthoclase is associated with
quartz, liornbleade, and mica; glassy felspar either with lioniblcnde
aud a black mica or with nugite ; labradorite with augite, vcrj
rarely with quartz or hornblende.
The felspars ai^ best knowu from similar minerals by their hard-
ness (they scarce scratch with a good knife), diflicult fusibility, and
unequal cleavages. The following marks may aid the student in
distinguishing the moro common species. In orthoclase the basal
cleavage plane forms a right angle with the clinodiagonal cleavage
planes it on both hands ; in the triclinic or pingioclaso felspars
tlie angles are unequal. Orthoclase, albite, andesine, and oligoolaso
are insoluble in acids ; labradorite and anorthite are more or Icsa
soluble. In granite, when decomposing, orthoclaso often become*
reddish or dark-red ; oligoclase dull greeu, and at length white. • 4
Walterhausen considers that the felspars are mixtures of three true
species, forming a scries with the oxygen of tOie silica, alumina, an*
BO in the pi-oportious z : 3 : 1,— j: ranging from 24 to 4. Tcher-
MINERALOGY
419
faak and most mineralogists now tase a similar riew, regarding
orthocUsa, albite, and anorthito alone as trae species, of which the
others are mixtures. Those consisting essentially of potash and soda
only are mechanical mixtures of ortlioclaae and albite, the distinct
lamells being visible by the toicroscope ; those again that contain
aaMntially limo and soda together are, sometimes at least, chemical,
being isombrphoos compounds of albite and anorthita in varions
proportions, and with corresponding transitions in crystallographic
ana physical properties. Notwithstanding this, these intermediates
most be regarded as independent mineral species, inasmuch as they
•n seTeralfy typical of certain rocks, and have characteristic forms
differing from each other in angular inclination.
689. Obthoclase, 'ilSij'+feSi,.
Obliciue prismatic, C- 63° 67': ooP (Tand /) llS" 47' ; P°" (i)
K' iff ; JP'eo (n) 90" 71'; 2poco (y)35°4B'. The commonest and
mmplest forms ai« ooP, OP, Pooo , and ooPoo (Jf), <»P, OP (P),
2P»iio (figs. 620 to 627). WTien ooP predominates the crystals
Ilg. 520.
Fig. 523.
are short rhombic prisma ;
when ooP*oo predominates
they are tabular; when
ooP and ooP*oo predomi-
nate they are short hexa-
gonal prismatic, when OP
and <»P"oo they are rect-
angular prismatic, often
mncfa lengthened. Twins
are very frequent, and
occnr according primarily
to four laws. Firtt,
Fig. 627.
Fig. 626.
through revolution of one half or of a whole crystal, then forming
interpenetrating twins round a vertical axis (fig. 195). In the case
of thia homitropic revolution one of the external faces becomes a
face of union. According as the right or the left half (or whole
crystal) is conceived to be that which has been revolved the crystals
are termed right and left, as in figs. 168, 189. Second, by revolution
of one half around an axis normal to Jf ; in such twins the com-
position is not evidenced externally except by sutures. Third,
Fig. 528.
Fig. 529.
Fig. 63a
through revolution round an axis normal to P, forming orthorhombio
prisms which show a herring-bone lineation, through the meeting of
stria commonly present upon the face .J/^ parallel to the intersection
of its edge with the face T (fig. 628). Fourth, by revolution round
an axis normal to 2P'm (n) ; this also forms a prism the section of
which is nearly square (fig. 529). Compound twins on thia last
type are formed of 3 to 4 and 8 crystals (Bg. 53o),
Occurs also massive, and coarse or fine granular. CL basal (P),
■nry perfect; clinodlagonal {IT), perfect {P : ^{-»0^ ; fracture
conchoidal or splintery. H. -6 ; G. -2-53 to 2-58. Transparent
to translucent on the edges ; vitreous but pearly on cl. ; and also
opalescent, with bluish or changing colours. Occasionally colour-
less bat generally red, yellow, grey, or green. B,B. fuses with
difBcnlty to an opaque vesicular glass. Kot affected by acidsL C. & :
64-8 silica, 186 alumina, and 16-9 potash, but generally 10 to 14
potash, 1 to 4 soda, 0 to 1-3 lime, 0 to 2 iron peroxide. Varietiea
are —
(1) Adularia and lu-spar, transparent or translucent, splendent,
and almost colourless. Some with bluish opalescence are named
Moonstone ; St Gotthard, Mont Blanc, DaapKiniS, Arendal, Green-
land, and Ceylon.
(2) Common Felspar, generally white or red, especially flesh-red,
is a common constituent of many rocks. Crystals at Baveno on
Lago Maggiore, Lomnitz in Silesia, Mourne Mountains and Wick-
low in Ireland, Aberdcnshire (at Rubislaw 6 or 8 inches long) in
Scotland, and at Carlsbad and Elnbogen in Bohemia. Amason
Stojie, verdigris-green, from Sutherland, Lake Ilmen, and Colorado,
and MurchisoniU, golden or greyish yellow, from Arran and Dawliah,
are varieties.
(3) The Glassy Felspar or Eanidine (C 64° 1', ooP 119° 16'j con-
tains 3 to 12 potash and 3 to 10 soda. Crystals imbedded ;
vitreous, translucent, and often mnch cracked ; Arran, £igg, and
other parte of Scotland, Drachenfels, Anvergne, and other countries.
Orthoclase occurs in granite, gneiss, and porphyry in many
countries. It is commonly associated with quartz ; sometimes, as
in the Graphic Granite of Sutherland, Harris, and Portsoy, in
letter-like combinations of the latter. It is very liable to decom-
position, when it is converted especially into kaolin, used for
manufacturing porcelain and stoneware. The adularia or moon-
stone and the green amazon stone are cut as ornamental stones.
LecliU, from Biddean nam Bian in Argyllshire and Grvthyttan in
Sweden, is a somewhat siliceous homy-lustred flesh-coloured com-
pact variety. Petunize and Eornstons are similar but more impure.
Microchns is a variety with angle distorted by interstitial penijtra-
tion, by oligoclase (Sutherland), and by albite (Frederiksvani. (cc).J
590. Albite, AlSi, + SaSi,.
Anorthic. OP (P) : o>I>«> (If) 86° 24'; ooP' (0 : o>'P {T) 122° IB';
bat angles variable. Crystals, generally like those of orthoclase,
are tabular or prismatic (ng. 197). Hemitropes common, especially
united by a face of oo^oo (figs. 631, 632) the re-entering angle b^
Fig. 631.
Fig. 58a
tween the faces of OP {P and P) 172° 48' being very chsracteristie.
Fig. 198 is another common hemitrope. Also massive, and in radiat-
ing plates. Cl. basal and brachydiagonal, almost equally perfect ;
fracture conchoidal or uneven. H. — 6 to 6*5; G. — 2"6 to 2'67.
Rarely transparent ; vitreous, pearly on the cL Colourless, but
fenerally white, grey, ^en, red. or yellow; streak white. B. B.
ifficultly fusible,
tinging the flame
yellow, to a white
semiopaque glass.
Not affected by
acids. C.c. : 68 6
silica, 19 '6aluroina
with O'l to 1 iron
peroxide, and 11 '8 _
soda, with 0 3 to 4 Fig. 633.
lime, 0 to 2 '6 potash. Hence albite and orthoclase both contain
soda and potash, only in different proportions. Albite is most
easily recognized by its frequent re-entering angles, its readier
fusibility, and the obliquity (93° 36') of its cl. planes, often marked
with striis. Pericline is a variety of which fig. 633 is a typical
form.
Albite is a constituent of many " greenstones," as at Corstorphine
(Edinburgh), and of granite, syenite, gneiss, porphyry, and trachyte.
Crystallized at Murdoch's Cairn, Aberdeenshire, being the colourless
felspar of the red granites of Scotland. Dauphine^ St Gotthard,
Tyrol, Salzburg, and Arendal.
Adinole is a compact variety similar in appearance' to Lceliic
691. Anobthite, ilSi + CaSi .
Anorthic. OP {P) : c»f «o (Jlf) 85° 60' ; aP" (1) : oo'P(T) 1»'
30'. Hemitropes common on both it and P. Angle between P
and f 180° 24'. CL basal and bltchydiaganal, perfect H.-S ;
420
MIJTERALOGY
0. — 27 to 278. Transparent ortransluoont J vjtr.cu3. Colourleeeor
white. B. B. fuses to a clear glass ; soluble without gelatinizing in
con. b. acid. O.c. : 4S silica, 36 '9 alumina, 20 1 lima sometimes
Fig. 635.
Fig. 634.
with magnesia and soda. Fetlar in Shetland j Lendalfoot in Ayr-
shire, in gabbro; Monte Somma, Iceland, Java. Lepolite and Am-
phodtliie are varieties. In Latrolitc the greater part of the lime is
replaced by potash. Glen Gairn and Labrador. At both roso-red.
592. OuoociASE, 2AlSi3 + (j5fa, 6a)jSij.
Anorthic. OP : oof <o 86° 10'; mF : oo'P 120° 42'. Hemitropes
face m, ivith p :/ 173° 4'; l -.1 120° 20'; i/:yl79°9'; x^:x 176° 69'.
CI. basal, perfect; brachydiagonal, less so. H. =6; G. «2'62 to 2 '84.
Vitreous, resinous on the cl. White, with a tinge of green, grey,
or red. B. B. melts easier than orthoclase or albite to a clear glass ;
not affected by acids. C.c. : 63 silica, 234 alumina, 8'4 soda, and
4-2 lime; thus nearly -3 albite and 1 anorthite. Distinguished
from orthociasa by the n.arked stris on the faces ; less readily from
albite, but more fusible and G. higher. The common associate of
orthoclase in the Scotch grey granites, especially in vein granite, as
at Kispond and Ben Loyal (figs. 536, 5371 =" "-"—'—' -' -'
Sutherland, and at
Fig. 536.
Fig. 637.
Rubialaw ; Scandinavia, Urals, Harz, and North America. The
SunstonCf from Foinaven in Sutherland, Norway, Lake Baikal, and
Ceylon, with a play of colour due to imbedded crystals of rubin-
glimmer (gbthite), belongs to this species.
693. Labeadoeite, Al'Si3 + (Ca, i{a)Si.
Anorthic. OP : <xf «= 86° 40' ; OP : ooT 111° ; OP : »P 113°
34'; ooP': oo'P 121° 37' ; a>f>» : ocP' 120° 63'; cxPor. : oo'P 117°
80'. Hemitropes of three types : — (1) according to the first law of
orthoclase as in fig. 638 ; that is, vertical revolution and face of
union ojfoo ; (2)revolutionof one half with reunion on the face ooPco,
Eig. 638.
Fig. 639.
Fig. 640.
as in fig. 539 ; (3) with twin face P, as in fig. 640. Hemitropes of
the last form also occur in which the lower naif consists of a hcmi-
trope formed according to the second method. Crvatals imbedded
in rocks consist generally of repeated twixa affording an angle o{
173° 20'. Cl. basal, perfect; brachydiaguual, less so ; both asnally
striated on account of the above twinning. H.— 6; G. — 2'38to2 74.
Translucent; vitreous, on the cl. resinous. Grey, passing into white,
green, yellow, or red. The faces of oof to often exhibit very beauti-
ful changing colours — blue, green, yellow, red, or brown — some-
times bands intersecting at certain angles. B.B. fuses more readily
than orthoclase to a compact colourless glass. Sol. in h. acid. C.c :
62-9 silica, 30-3 alumina, 123 lime, and 4'5 soda. It is thus-1
albite and 3 anorthite. Common constituent of dolerite, gabbro,
and hypersthene rocks. In Scotland, Labrador, Finland, Harz,
Tyrol ; also at Etna and Vesuvius.
594. Andesine, AlSi3+(SaCa)Si.
Anorthic. Crystals similar to albite and anorthite. Twin face
M. Crystals generally formed of repeated plates. G.-2-67to27.
Physical properties like albite; more easily fusible to a porous white
glass ; h. acid sometimes dissolves out alternate laminte of crystals.
C. c. : 59 7 silica, 25 6 alumina, 7 7 soda, and 7 lime, and thus nearly
1 of albite and 1 anorthite. Typical of the primary limestones
and a granitic belt therein in Scotland, as at Shinness, Urquhart,
Dalnain, &c. In the Andes, the Vosges, and Iceland.
'695. Hyalophane, 'ilSij, KS'ia + ilSi, BaSi.
Oblique prismatic ; resembles orthoclase ; crystals and angles
nearly the same. Cl. OP, perfect. H. -6 to 6-5 ; G. -2 '8 to 2-9.
Transparent. Lustre vitreous. Colourless, white, and fiesh-red.
C.c: silica 527, alumina 21, baryta 15'1, potash 7'8, soda 21.
B. B. difficultly fusible to a blobby glass, not acted upon by acids.
Binnen in Valais, Jacobsberg in Sweden.
596. Barsovite, AlSi-hCaSi.
Right prismatic, or oblique prismatic. H. = 5'6 to 6 ; G. =2 '58.
Snow-white; translucent. Fracture granular. Pearly. C.c. : silica
42 '2, alumina 36-4, lime 19-8. Gelatinizes in h. acid, difficultly
fusible. A dimorphic form of anorthite. Barsovskoi in the Urals.
597. Sadsscrite.
A massive, granular, translucent, white or pale green felspathic
mineral of the nature of anorthite mixed with labradorite. H. = 6 to
7; G. = 3'26 to 3"4. Probably a mixture. Occurs in loose blocks neat
Geneva,, and in Corsica. In China and in India is carved under the
name of Oriental jade (nephrite). Seems to he confounded also
with zoizite, and perhaps with yii (prehnite). JadciU is similar.
Zeolite Geodp.
These crystallize in all the systems except the anorthic, and them-
selves present great variety of development. Mostly hyaline and
white ; rarely red, grey, or yellow. Cl. generally distinct. All
yield water in closed tube ; all fusible B.B. most easily, and often
intumescing ; all sol. in acids, and mostly gelatinize or deposit
silica. They are hydrated S'licates of alkalies, or alkaline earths,
mostly with silicates of alumina, but rarely contain magnesia.
Some minetalogists regard the water as basic, in union with silica,
and Kenngott gives the formula in that form, thus ; —
Analcime, (ifaAl) 2Si-H2(fi, Si),
Natrolite, (SaAl) 2Si-f2(fi, Si),
Stilbite, C^a, ■Al+6{li, Si),
and the othei-s similar. They are generally found in amygdaloidal
cavities or fissures of trap or jilutonic rocks, apparently as deposits
from water percolating into inem, and are thus probably products
of decomposing nepheline or felspars, or hydrated felspars them-
selves. They never form constituents of rocks. Natrolite,
scolezite, thomsonite, and the connected varieties are marked by
their needle-like radiating forms ; stilbite and heulandite by their
broad, foliated, pearly cleavage,
698. Pectolite, 4(iaSi + ?<aSi2-l-H.
Oblique prismatic, C 84° 37'. ooPoo (c) ; OP («) 95' 23'. Cl. c
and u. Twin-face c ; chiefly spher-
oidal and radiating fibrous. H. — 5;
G. -274 to 2-88. Translucent;
crystals pearly ; fibres silky. Pale
green to yellowish white. Sol. in
h. acid, leaving silica. C.c: 54*2
silica, 33 7 lime, 9 4 soda, and
27 water. Katho, Corstorphine, Castle Rock,
Edinburgh; Kilsyth, Stirling ; Knockdolit
shire; Skyo ; Montebaldo ; Monzooi Valley in Tyrol.
569. Walkertte, 4C'aSi + Xlg§i + Sa§i, + 2H.
Like pectolite, but columnar. H. — 4'5 ; G. = 27. Flesh-coloure-l.
Lustre pearly to greasy. C c. : silica 537, lime 28*6, magnesia
6 1, soda 7 9, water 4 '6. Corstorphine Hill, Bumtislandi '''
600. Xosotlite, 4Ca§i-fS.
Uossivc. H. -6; 0.-2-6 to 27. Pink, white, and grey. Tough;
Fig. 541
nd Arthur's Seat,
nd Lendalfoot, Ayr-
MIKEEALOGY
421
fiitare conclioidal and splinferv. C.c: silica. 49 S, liiue 43 5,
cr^toiide of mangmese 2'3, protoxide, of iron 2 '9, water 8 7.
JCiiinichec and Torosaj (UiiU). Xonotla (Mexico),
601. ToBEBMOBrri, 3(0a^. ft)Sij + 2>.S.
Massive, fine granular; translucent; fracture hacklr. H. — F;
G -2-4. Pale pink. C.c. 'silica 4p-8, lime 87-2, water 12 9.
Tobermory (Hull}, Dnnvegan (Skye)
602. OKzyiTE, CafiSi, + S.
Right prismatic. ocP 122' 19'. Usually fine fibrous; radiatine.
H. -6; G. -2-28 to 2 36 Pellucid; slightly pearly. Yellowisli
to bluish white. In powder easily sol in h. acid> leaving
gelatinous fiakes after ignition. C.c. : 66 8 silica, 28 4 lime, and
17 water ; an apopbyllite without the fluorine. Disco Island,
Faroes, and Iceland.
603. ApopHTLLrTE, 8(6aSi + 2S) + KF .
PyiamidaL P 120° 56'. P, ooPoo (m), OP (t>), ocP2 (r).
Rarely lamellar. CI. o, perfect Brittle. H. — 4'6 to 6;
G. — 2'3to 3-4. Transparent; vitreous. On o pearly (/cA/^yo/:^-
thalmiU). Colourless, rarely pink, green, red, brown, and yellow.
B.B. exfoliates, intumesces, and melts to white enameL SoL in
b. acid, leaving silica. C.c: silica 50 '3. lime 247, water 15 'P,
Fig. 642.
Fig. 643.
Fig. 644.
potassium 4'3, fluorine 2'1. Dunvegan and Storr, Skye (fig. 644);
Chapel, Fife ; Corstorphine (fig. 542) and Ratbo, near Edinburgh ;
Kilsyth, Bowling, Kilpatrick ; Port Rush, Ireland. In the form
P (fig. 79), grass-green at Oxhaveer, Iceland {Oxhaveerile) ; Utb,
Sweden ; Audreasberg and Faroes (pink) ; Faroes, and Poonah in
India (green). Internal structcre tesselated, being built up of wedge
?.nd lenticular forms with varying refractive indices, hence exhibit-
irig a beautiful structure with poiarized light.
604. Gteolite, (jCa + jS)Si-f-H.
Lamellar, radiate, spherical, and investing. H. =- 3 to 4. Pearly.
Bluish white to cream-coloured. Transparent, rapidly becoming
cpaque. C.c: silica 533, lime 329, water 13'8. Quiraing,
Ljadale, and Storr, Skye; Loch Screden and Carsaig, Mull ; Canna;
Karartut, Niakomak, and Disco ; Faroes ; Nova Scotia.
605. Analcime, ilSi, + 5^aSi + 2fi .
Cubic. ooO<«;;202. Fracture uneven. H.-5'5 ; G. -2'1 to 2-28.
Colourless, white, flesh-red, scar-
let. Vitreous; transparent. B.B.
melts without frothing to a clear
vesicular glass. Decomposable
with gelatinization in h. acid.
C.c. : 64-5 silica, 23-3 alumina,
141 soda, 82 water. Walls,
Orkney; Talisker, Skye; Sanda,
and Hebrides generally. Trans-
parent at Eigg, and Elie, Fife
scarlet at Bowdens, Kincai*dine ;
opaque white at Glen Farg,
Salisbury Crags, and Dumbarton;
Giant's Causeway, Seisser Alp in Fig. 545.
Tyrol, Cyclopean Islands (fig. 545), Faroes. Iceland, and Nova
Scotia. EudnophiU is a variety. Fecto-
lite (sp. 698) occurs pseudomorpbous after
analcirae, in large crystals of a, «, at
JRatho, Edinburghshire.
006. PoLLtTX, 8("AlSi, + (6s}, Sa})Si)-f
Cubic ooOoo; 202 (fig. 646). Also
massive. Gum. like externally. Brittle,
^th traces of cleavage. Fracture con-
choidal. H. -5o to 6-6; G. - 286 to
29. Colourless. Vitreous. Sol. in n. i. ,.. , .„,
acid. C.c. : silica 44, alumina 16, oxide ''^- °^® ^'P' ***''
of cRsium 34, soda 2'5, water 2*1. Elba. ^The only mineral which
contains c«sium in (juaatity.
607. FAFjABrre, i&^i\t+{.ta^)^i,^XZli.
Cubic : in octahedrons with the icositetrahedron ^Of Fracture
uneven; brittle H. -7 ; G. -1-92. Transparent; vitreous to
adamantine White to brown. Sol. in h. acid. C.c: 46-8 sUica,
16 alumina. 4 4 lime, 4 8 soda, 28 water. Kaiserstnhl in Baden,
Annerod near Giessen, Eisenach, Marburg.
608. Chab.\site {Lime-Clwbasite), ftlSij -I- CaSi -I- 6H .
Rhombohedral : K 94° 46.' KR4 ;-lR (r) ;-2R (e) ;
Twin." very common (generally interaesting).
Fig. 647. Fig. 548.
Poo . Primary rhombohedron is sometimes twinned with a crystal
with faces r, «, j. CI r perfect H. -4 to 4-5; G. -2 to 2 2.
Transparent or translucent; vitreous. Colourless, and brownishl
Fig. 649. Fig. 650.
yellowish, brick-, and flesh-red. SoL in h, acid, leaving silica.
C.c: silica 47-8, alumina 20'8, lime 107, water 21 3. Lyndale
(figs. 647, 648. 649), Talisker (figs. 176, 660, sometimes flesh
Fig. 551. Fi^. 552.
colour), and Storr, Skye (figs. 647, 548); Port Glasgow and Kil-
malcolm (pink and brown) ; Giant's Causeway and Magee Island
(red), Faroes, Iceland,
Aussig, Audreasberg
(fig. 551). Baydtnite in
twinned rhonibohedra,
with p:p 95° to 97° and
2> : d 170° reentering (fig.
552), from Fassa and
Maryland, is similar.
FkacoliU is chabasite in
twins of JP2, o=P2, R,
-iR at the Giant's
Causeway (fig. 154). At
Richmond in Victoria _. ,,„
thpv rw-riir Bs in fitr ''6' ^''"*
653, - 2R (n), - JR (r),'}P2 (i), OP (e) ; polar edge,'}P2 146'. . In
this, half of the lune is replaced by soda.
609. GuKLKJITE(5oda-CTa6ari(<), AiSi,-f}>aSi-(-6S.
Hexagonal R 112° 26' ; P 78° 64'. Combination P, ■OP'.'^P,
422
MINERALOGY
(figa 554, 556). Faces of P striated paiiJlel to the polar edse, those
of the prism horkontally {fig. 655). CL ooP distinct. Gelalinizes
Fig. 557.
Fig. 558 (sp. 611).
86. Aci-
Fig. 656.
with h. acid. C.c. : 47'6 silica,
197 alumina, 12 soda, 207 water.
'-' Certain crystals seem to indicate
twinning-. Talisfcer in Skye (twins of iig. 665), Glenaim in
Antrim (Cg. 655), Vicenza, Pyrgo
in Cyprus, Cape Biomidon in Nova
Scotia.
610. IiETTNE, iilSij + CaSi +
as.
Khombohedral ; P, (s) 79° 29' ;
-JR (r) 106=3'; OR (o). Forms
intersecting twins as in fig. 557.
H. = 4; G.-2-1 to 2-2. Colourless
and white. Co.: silica 4S'8, alumina 23"8, lime 97, water 21.
Storr in Skye (o, s), Ireland (at ,
Glenarm, Island Magee, London-
derry, &c.), Iceland, Dalsnypen,
and Naalsii in the Faroes.
611. Hekschelite, 'itlSia +
(6aNa)Si + 6H.
Hesagonol prisms (e) snnnounted
by two trihedral pyramids of a, and
one of ffiV(fig- 558). a, : e 122° 8' ;
a" : c 107° 26'; e striated hori-
zontally. CI. e ; fracture con-
choidal ; transparent ; vitreous.
White or colourless, H.=5-5;
G. = 2-06. C.c: silica 47, alu-
mina 21"2, lime 5'2, soda 4'8, potash 2, water 17'
Castello and Palagonia in Sicily, Yarra in Australia.
612. Laumontite (^Leonhardile), iiciS'i3-HCaSi-K4H.
Obliiiue prismatic, C 80° 42'. ooP (m) 86° 16'. ooP:- ooP («)
113°30';Poo (x,):- ooP 111° 14' ; e : «125°41';
o:S 90° ; e : z 149° 15'. Twin face a. CI. m,
perfect; very brittle. H. = 3 to 3-5; G. = 2-2
to 2'3. Pellucid when fresh ; vitreous ; pearly
on cl. White, cream-coloured, brick-red. De-
composes rapidly through loss of water. B.B.
intumcsces, and melts first to a white enamel,
ultimately to a clear glass. Gelatinizes in h.
acid. C.c: silica 60'9, alumina 21 '8, lime
11 '9, water 16 S. Rapidly loses 1 equivalent
or 3 '86 per cent, of water, and becomes fri-
able (Eypostilhite). Kilfiniohen, Mull (fig.
559) ; Storr and Quiraing, Skye (hypostil- \ k. -s k
bite); Tod Head, Snizort, Glcu Farg (red); \^ I'V;^
Bowling, Dumbarton (twins of m, e) ; Hnel- ^ — ^^^
goat in Brittany ; Prague, Falun, Iceland, ^'E- ^•"•
Faroes, Nova Scotia. Caporcianite from Tuscany has only 3
water.
613. Epistileite {Reiasite),
JUSij-hCaSij-hSfi.
Oblique prismatic, C 64° 63'.
ooP (m) 135° 10'; Pco («) 109°
46'; iP(s)147°40'(Cg.560). Hemi-
tropes united by m, with twins of
the same united by the brachy-
diagonal (a). CL brachydingonal,
perioct. II. -3-5 to 4; G. -2-3 to
2 '4. Pellucid; vitreous; pearly
on cl. Colourless. Sol. without
gelatinizing, C.c. ; silica 59, alum-
ina 17 '5, Ume 9, soda 1'5, water ^, rfn
14-5. Talisker in Skye (m, «, o); rig. uou.
Hartlepool (in twins), Iceland, Faroes, Silesia, Tiesch in Vabis,
^ova Scotia, and New Jersey.
614. Heulandite, AlSi3 + (5aSi3-!-533E.
Oblique prismatic, C 63° 40'. P'oo (?) SO" 20' ; 2P (z) ; |P («) ;
2P«oo (r) ; 3PCCO (s) ; aV<o ; ooF; OP. 2 : s 136° i';u:u 146° 52'..
Crystals elongated along
each of the axes pre-
sent very varj-ing forms,
but generally tabular
Cl. clinodiagonal, per-
fect ; pearly on this,
vitreous on others ;
brittle. H. =3-5 to 4;
G. =2-lto2-2. Trans-
parent to translucent ;
colourless, while, brick-
red, rose, green, hair-
brown. B.B, melts with
exfoliation and intu-
mescence to a white
enamel, Sol, in h.
acid, leaving silica.
Storr and Taliskcr,
Skye (fig. 562) ; Sanda;
Kilmalcolm; Catterline,
Kincardine (fig. 563) ;
Kilpatrick HiUs (p, m,
n, z, u, r, s) and Kintyre
(red) ; Iceland, Faroes,
Fig. 565.
Fig. 564.
Fassai Valley, Nova Scotia, Baltimore {BeaumonliU) (fig. 665)
(T?, m, n, s, t) ; Vindhya Mountains in India (fig. 564),
615. Brewstekite, 'AJSi3-i-RSi3+5S, K=(fSr-h0a-f-}<5a).
Oblique prismatic, C 86° 56'. ooP°oo (a) ; «?=«; (I) ; "tlP (o) ;
kP'oo (e); ooP (m); coP»2 (c); ooP'f (<). e:e
173° 10' (fig. 566). Cl. clinodiagonal, perfect ;
pearly on do,, vitreous on others; pellucid.
H, =6 to 5-5; G. =2-5 to 2-46. Colourless,
yellow, or brown. Sol. with gelatiuization in h.
acid. C.c: 54*3 sUica, 15 alumina, 9 strontia,
6 '6 baryta, 1'3 lime, 13 '5 water. Strontian,
Freiburg in the Breisgau, Pyrenees.
610. Phillipsite, A!Si3 + (Ca, K)Si-)-5H,
Oblique prismatic, C 55° 1', ojP (m) ;
ooP'^oo (i) ; OP (c). Polar edges 120° 42' and
119° IS', Faces b and 7/1 striated parallel to
the intersections. Apparently always twinned ;
generally these duplicated by intersection on
lace b or face c (figs. 507, 668), and frequently "S- 666 (sp. 615).
arranged so that three of the above double tivins intersect at
right angles to one another, forming the cruciform fig. 569.
Fig. 669. Fig. 670.
When the prismatic faces of these are short, the faces m of the
MINERALOGY
423
iot«tsacting individoals fall nearly into one plane, presenting the
form fig. 670 ; when long, fig. 190. Brittle ; fracture uneven.
H. -.4-5; G. -215 to 2-2. Gelatinizes in h. acid. C.c: Bilici48-6,
alumina 20-2, lime 7'3, potash 6-2, water 177. Giant's Causeway,
Giessen, Marburg, Cosset, Capo di Bove, VesuWus, Iceland.
617. Habmotome, AJSij + BaSij+Sfi.
Oblique prismatic, C 55° 10'. ooP (j) ; ooP oo (b) ; OP (a).
Forms like phillipsite, but more frequently in simple twins.
Physical properties like phillipsite, but G. — 2 3 to 25, and fuses
Fig. 573. Fig. 574.
with difficulty. Difficultly sol. in h. acid. C.c. : 46 5 silica, 15-9
alumina, 23 '7 baryta, and 13 '9 water. Strontian, transparent
(Morvmile, fig. 572) and opaqUB (figs. 671, 573); Glen ArbucK (fig.
674) and Bowling in Bumliarton ; Corstorphine near Edinburgh ;
Audreasberg, Kongsbcrg, Obci-stein.
«18. Stilbite, AlSij + CaSij + eS.
Oblique prismatic, but with right prismatic habit; C B0° 49'-
00^00 (a) ; ooPoD (i) ; P (r) ; c»P2 (m) ; OP (p). CI. a, perfect.
H. = 3 -5 to 4 ; G. - 2-1 to 2 2. Transparent ; vitre-
ous. Pearly on a. Colourless, white, yellow, pale
brown, biick-red. Decomposed by h. acid, leaving
silica. C.e. : silica 57o, alumina 16'4, lime 89
water 17-2. Storr and Talisker in Skye (a, t, pi
(Eg. 576), and in Hebrides (colourless) ; Arrau and
KUmalcolm (pale brown) ; Long Craig (Dumbarton)
and Kinneff (Kincardine) (brick-red) ; Iceland,
Faroes, Andreasberg.Vindbyailountains, Wellington
Uountains (Austr.'Jia), Nova Scotia.
619. PiTFFLEr.iTE, Ais\ + Ca./ij + sS.
Fibrous globular concretions, with vitreous surface.
H.-.4; G. -2-21. Greyish white. Transparent.
C.C.: silica 52-8, alumina 16-3, lime 11% water
17-2. Pufflatsch iu the Scisser Alp.
620. Edikoto.vite, 4AlSi;-H3riaSi + 12a.
Pyriftnidal ; hcmihcdral with inclined faces. P 87° 19' : JP (re)
129* 8' ; ooP (a) ; polar edges _._
P 92° 51' (fig. 57G). CI. a, j
feet ; fracture 'inevcn. H.
to 4-5; G. -2-7 to 271. Trans
lucent ; vitreous. Colourless.
C.c: silica 37-3, alumina 2375,
baryta 26 -52, water 12 46. Kil
Patrick Hills in Dumbarton
shire.
621. FoRESiTE, i&aii,
•■K^Ci,1Sh + 6& Fig. 576* (sp. 620).
Kight prismatic. ooPoo ; ooPoo ; OP. CI. brachydiagonal,
perfect ; lustre thereon pearly. G. =.2'4. White. C.c: silica
60, alumina 27 4, lime 5j, soda 1-4, water 16 1. San Piero
*iElba.
622. NATROinx, AlSi, + SaSi-f2fi.
Sight prismatic. ooP (m) 91° ; P (o) j polar edges 148° 20' and
.144° 40', middle edge 68° 20' j oof « (i) ; ocP« (o). Radiating
aoicular crs'Stals, often fibrous. CL ojP, perfect H. -5to 6-5 ;
"j. =217 to 226. Pellucid: vitreous. Colourless, ochre-yellow,
reddish. Is not pyroelectric. B.B. melts quietly to a clear glass,
colouring flame yellow. SoL in oxalic acid. " " '"'" "''""
Fig. 577. Fig. 578.
27 alumina, 16-3 soda, 9-4 water. Glen Farg (fig. 577), (colourless
and reddish), Tantallon Castle (fig. 678), Dumbarton, Bowling
(greetf), Campsie, Bishopton, Glenarm and Port Rush (Ireland),
Auvergne, Hesse, Hohentwiel in Swabia, Norway. CrocalUc is red,
fibrous, and investing ; Kintyre, Forfarshire, Wemyss Bay. and the
Urals.
623. SCOLECITE, AlSij -1- CaSi -I- 3H .
Oblique prismatic, C 89° 6'. osP (m) 91° 35' ; P (o) 144°
20 ; - P. Prismatic and acicular crystals. 'Twins common, on face
00 P'oo, one face with feathered strias. CL ooP, perfect. H. — 5to
6-6; G. =2-2 to 23. Pellucid ; vitreous ; pyro-electric Wliite
to reddish white. B.B. twists in a vermicular manner; melting
readily to a porous glass. Only par-
tially soL in oxalic acid. C.c. : silica
45-8, alumina 26-2, lime 14-3, water
137. Staffa; Loch Screden, MuU ;
Talisker, Skye ; Berufiord, Iceland
(fig. 679); Faroes; Vindhyas, India.
Natrolite and scolecite pass into one
another. There are two definite in-
termediates— Fargite, consisting of
two equivalents of natrolite and one
of scolecite, and Mesolite, consisting
of one of the former and two of the
latter. The first of these occurs
at Glen Farg and at Bishopton
{GalactiU) ; the second is the ordi-
nary radiated zeolite of the amygda- Fig. 579.
loids of the Tertiary igneous rocks of the Hebrides and the Farces.
It there occurs in matted crystals of extreme tenuity {Cotton-
sto:ie), also in delicate feathery tufts ; in Renfrewshire in spheres
with an internally radiated stmcturo, and also in needle form and
in downy tufts.
624. GisMONDiNE, AlSi-hCaSi-f-4fi.
Pyramidal. P (6) 92° 30' : polar angle 118° 34' ; ooPa
580). CI. P. H. -5, on edge/
and angles 5 to 6; G. -2 26.
Translucent ; vitreous. Bluish
white to pale red, C.c: silica
36-9, alumina 273, lime 131,
potash 2 '3, water 21 1. Island
Mageoaiid Larue, Ireland; Vesu-
vius, Aci-Cadtello, and Capo di
Bove ; SchiHenberg near Giessen ;
Schlauroth near Gorlitz.
625. Zeaooniie, AlSi + (CaSJ
Si + 4SE.
Right prismatic. P polar angle 120° 37' and 121° 44' ; middle
angle 89° 13'. Crystals like fig. il9. H. —6, on edges and angles
7; G. =2-3. Transparent ; vitreous. Colourless, ^
white, or bluish. C.c: silica 44, alumina 23*3, "'" ' " ^'^
lime 5'3, potash 11"1, water i5"3. CapodiBove
626. Thomsoxite, 2AlSi-H2(CaNa)Si + 5fi.
Right prismatic o>P (m) 90° 26' ; osPoo (a);
cx.f=o (6) ; ipoo (!,); Pco (r) ; ^Poo (x). X : X
177° 34' 20". CI. macrodiagonal and brachy-
diagonal, both perfect. H. -5 to 55 ; 0.-235
to 2 '38. Translucent; vitreous; pearly on mac-
rodia^onaL Colourless. B.B. difficultly fusible
with intumescence to a white enamel. Sol. with j'j-^ ggj /gp_ q2Q).
gelatinization in h. acid. C.c : silica 387,
alumina 30-8, lime 13-4, soda 4-4, water 13-1. Lochwinnoch,
Renfrew ; Eilpatrick (fig. 68"^ • Quiraing and Talisker {sometimes
Fig. 680.
424
MINERALOGY
massive-granulsr) ; Rathlin ani Ma^^ee Island, Ireland;
Vesuvius (fig, 581), Sicily, Bohemia, Tyrol,
Nova Scotia.
FaroeliU is a variety with 42*5 of silica.
It replaces thomsonite generally in Tertiary
igneous rocks, occurring at Storr and else-
where in the Hebrides, Faroes, Iceland,
and Nova Scotia. The angle of the vertical
prism is within 8' of that of thomsonite. It
contain? an equiv<aleut more silica.
627. Prehnite, AiSi + 2CaSi + fl .
Right prismatic. ooP (?n) 99° 68' ; OP
(c); 3poo (e)33°26'; JPoo (v)90°32'; ooPoo Fig. 682 (sp. 62
(a); oopco (i); P (s). Crystals either tabular of c, or prismatic
both the vertical and the brkchydiagonal axes, hence varying
in form. Also in fan-shaped and botryoidi^ aggregations,
perfect; pearly thereon, vitreous else-
where. H.-6 to 7; G. =2-8 to 3.
Transparent to translucent. Colour-
along
much
CI. c.
Fig. 683.
Fig. 664.
less, but generally green of bright but pale tints, also lemon-yellow.
Becomes electrically polar by heat. B.B. intumesces greatly,
melting to a porous enamel. Decomposed by h. acid. C.c. :
silica 43 '6, alumina 24 9, lime 27'1, water 4 '4. Glen Gairn, Aber-
deen (fig. 683) ; Skye and Mull ; Corstorphine Hill (green and
pink). Castle Rock (white), and Salisbury Crags (yellow), Edin-
burgh; Frisky Hall, Dumbartonshire (fig. '^84); Hartfield Moss,
Renfrew (botryoidal); Cornwall; Dauphine ; Tyrol: Cape of Good
Hope; China (Til).
628. Friedelite, MniSi3 + 2H.
Rhombohedral ; R 123° 42'. OR ; ooR. Tabular habit, and in
granular aggregates. CI. basal, perfect. H. = 4 to 6; G. —31. Rose-
red, with paler streak. C.c. : silica 36, proto.xide of manganese 63,
lime 2'96, water 7'9. Adervielle on the Neste de Louron (Pyrenees).
HrDKOUs Silicates of Alumina.
These are probably for the most part products of decomposition
of felspars under atmospheric exposure.
629. Kaolin {Porcelain Earth), 'A1&L + 2S.
Massive ; in beds and veins. Fracture uneven ; fine earthy, very
soft, seotile, and friable. H. = 1 ; G. - 2-2. Onaque, dull. White or
grey, inclining to blue, green, yellow, or red. Feels meagre, not
greasy when dry, and plastic when wet. B.B. infusible. Not
affected by h. acid, but decomposed by warm s. acid, leaving silici.
C.c. very variable, but approximates to 46 silica, 40 alumina, and
14 water. Chiefly a product of the decomposition of orthoclase, or
of granite, porphyry, and other rocks containing that mineral.
Cornwall and Devonshire in England are the chief European locali-
ties for the kaolin used in manufacturing porcelain.
Clays are merely varieties of kaolin, mixed with quartz-sand, car-
bonate of lime, magnesia, and the oxyhydrates of iron. Often 40
to 50 silica, 30 alumina, 13 to 20 water, and 4 iron peroxide,
with lime and potash. In the fire they are infusible, burning
hard. Generally tliey are compact and friable, of white, yellow,
red, blue, grey, or brown colours. Their specific gravity varies
from 1"8 to 2'7. The following are varieties. Pipe-chn/, greyish
or yellowi'^h white, with a greasy feel, adheres strongly to the
tongue, when wet is very plastic and tenacious, and in the fire
burns white. Al^nndant in DevonsliiiT, and in the Trough of
Poole in Doi-aetshire; in France, Belgium, and Gei-many. Used
for manufacturing tob.acco-pii»e3 and sinlilar articles. Poller s
Clatj, red, yellow, green, or blue, becoming yellow or red when
burnt ; more easily fused than the former, and often effervesces
with acids. That used in the potteries in England comes chiefly
from Devonshire. Loam, coarser end more impure, with more
sand, and consequently less plastic. Sfmlc or sLiU Clay, greyish
black, and much mixed with bituminous or carbonaceous
matter. Bituminous SJuili, known by its shining resinous streak.
Black Clialk, with more carbon, leaves a black mark on paper. Iron
Clay contains much peroxide of iron, is reddish-bro^n, and forms
the basis of many amygdaloids and porphyries.
630. Nacrite, itlSij-f2fi.
Right prismatic; minute six-sided tables in fan-like group ; and
scaly. H. - 0 -6 to 1 ; G. - 2 35 to 2 -6. GUmmeriog to pearly, snow.
whit« or yellowish white. C.c: silica 46'3, alumina 39 8, water
13 '9. A crystalline form of kaolin. Fins in Allier, Mons, Freiberg,
Pennsylvania, and coal formation commonly.
631. LiTHOMARQE.
Kaolinic substances, compact, earthy, and psendomorphoua.
H.-2-6to3; G.-2-4to2-6. White, yellow, or red. Greasy, adheres
to tongue. Klausthal, Harz, &c. Similar are Caniat, Myelin,
Mclopsite.
632. Hallotsite, !4'lSi-t-4S.
Massive and reniform. H. -1-6 to 2-5; G. -1-9 to 2-1. 'Trans-
lucent when moist. Bluish white,"green, or yellow. C.c. ; 41 "6 silica,
34 "4 alumina, 24*1 water. Hospital Quarry near Elgin, on the
Tweed, Liege, Tarnowitz, Eifel {tenziniu). Fuller's Earth may be
an impure ferruginous variety. Maxton in Scotland, Reigate and
Maidstone in England, Saxony, Bohemia, &c.
633. Glagerite, AljSij-f 6H.
H. — 1; G. — 2'35. Bergnersreutn. Mallhazile, from Steiniotte]
near Bautzen, has less alumina.
634. Kolltrite, 'iljSi-ngfi.
H. — 1 to 2; G. — 2. Also similar. Schemnitz, Pyrenees, and
Saxony. Scarbroite from Scarborough has lOHjO.
635. MiLoscHiN.
Conchoidal or earthy. H.=2;G.=2'1. Indigo-blue to celadon-
green ; has 2 to 4 chrome o.xlde. Rndnik in Servia.
636. MONTMORILLONITE, AljSij-f 2H.
Massive. Rose-red. Montmorillon and elsewhere in Fi-ance,
Poduruoj in Transylvania.
637. RAzocmoffskin, AlSij-l-SS.
From Carinthia. Chrome Ochre, with 2 to 10 per cent, of chrome
oxide, from Waldenburgin Silesia and Creusot in France, is similar.
638. CiMOLiTE, AljSij-f efi.
Pseudomorphous after augite. Ellin. Limburg, Kaiserstuhl,
Argeutiera and Milo.
639. Allophane, 'AJSi-f5H.
Botryoidal and reniform. Fracture conchoidal ; brittle. H. = 3 ;
G. — 1 8 to 2. Pellucid ; vitreous. Pale blue, white, green, or
brown. Colour due to copper. Charlton, Woolwich, Baden, and
Bonn.
640. Ptrophtllite, A'lSij-fS.
Right prismatic, but radiated, foliated. CI. perfect ; flexible,
sectile. H.^l; G.=2'8to2"9. Translucent, pearly. Lightverdi-
gris-green to yellowish white. B. B. swells up with many twistings
to a white infusible mass. C.c: 67 sUica, 28 alumina, and 5
water. Urals, Spa, Morbihan, Westana in Sweden, Carolina, and
Brazil. Talcosite, from Heathcote in Victoria, has silica and
alumina about equal.
641. Anauxite, 'i^lSij-f 3H.
Granular. H. -2 to 3 ; G. =2-2 to 2 '4. Translucent, pearly.
Greenish white. C.c: 60'6 silica 26 alumina, and 13-5 water.'
Bilin in Bohemia.
Hydrous Silicate.? of Zirconia, Thoria, fco.
642. Malaco-ne, SZrSi-ffi.
Pyramidal. P 83° 30'. Typical form ooPoo, P, t» P. H. -6;
G, — 3-9to4'l. Conchoidal fracture. Lustre vitreous. C.c. same
as zircon, but with 3 of water in the Hirteto variety and over 9 in
that from Finland. Has a surface opalescence, and may be altered
zircon. Hittcri), Chanteloube (near Limoges), ne
dal,.Finland, Miask.
613, EUCRASITE.
Right prismatic (t). H. -IS to 5 ; G. -43
Blackish brown ; streak brown. Translucent on edges. Fracture
uneven; brittle, C.c. very complex : silica 16, thoria 36, cerium
protoxide 5-6, peroxide 0, lanthania 2 4, yttria 4-8, erbia 16,
titanic acid IS, ferric oxide 4-25, alumina 1'8. water 9. Barkevig
near Brevig.
644. Thorite, ThSi-^ 28.
Pyramidal. ooP : P 133° 30'. Generally massive. H.-4-5
to 6. G.- 6 to 5 4. Lustre brilliant vitreous; when weathered
resinous. Fructuro conchoidal when fresh, Bplintcry when
weathered. Brownish black to clove brown. C.c, complex, but
•ascntially 18 silica, 73 thoria, 9 water. _ In syenite at Lochan
r Dresden, Rosen-
Lustre greasy.
MINERALOGY
425
Fig. 585 (sp. 644).
Hacon, asd ib a boulder on Ben Bhreck in Sutherland, in crystals
(fig. 585); Lowo near Brevig, Nor-
way. Vranothorite, from Arendal,
has SO per cent, thoria and 10 uianous
oxide ; found also at Uitteri^ and at
Champlain (TJ. S.)
645. Oeaugite, 8ThSi + 2fi7
Massive. Oran^e-yeliow to cinna-
mon-red. Other characters like tho-
rite, do. : 17 silica, 75 thoria, 7
water. Ben Bhreck, Langosund near
Brevig. The mineral from Ben Bhreck
passes gradually into thorite, which
thus would appear to be altered
orangite.
646. Teitouite, S2Sij + 4fi.
Cubic. In tetrahedra. H. = 5 '5 ;
G. =39 to 4 '66. Lustre vitreous.
Dull brown ; streak yellowish grey.
Siibtranslucent. C.c. complex: silica
21, aluciina 25, ceria 40, lanthania 15, yttria 4'6, lime 4, water 8.
Lu.ico nsar Brevig.
Maonesian Silicates.
647. AoALMATOLlTE (/Vyarc S((»m), 4'AlSio+ESi3 + 3i£.
Massive or slaty. Fracture splintery, rather sectile. H. =2to
3; G. =2'8 to 2'9. Tracslucent; glimmering. Green, giey, red, and
ycUow. Feels somewhat greasy, but does not adhere to the tongue.
Sol. in s. acid. C.c. : 55 silica, 33 alumina, 7'6 potash, and 5 water;
but in many localities magnesian. Calligaig in Sutherland ; China,
where it is cut into various works of art; also Nagyag in Hungary,
and Saxony.
648. Oncosin, 2^'lSij + (g,Mg)Si2 + 2H.
Fracture uneven or splintery; sectile. H. = 2;G. =2'8. Trans-
lucent; slightly resinous. Apple-green or brown. SoL ins. not in
h. acid. Salzburg.
649. Liebenerite.
Hexagonal. ooP ; OP. 01. prismatic, perfect ; fracture hackly.
H. = 3'5; G. =2'8. Oil-green, bluish green, and greenish grey.
Greasy lustre. C.c: silica 447, alumina 36"5, potash 9"9, water
6 '5. Monte Viesena near Forno, Predazzo in TyroL
650. GlESEOKITE.
Hexagonal. ooP; OP. Fracture splintery. H. =3to3-5; G. =2'7
to 2 9. Kangerdluarsuk in Greenland, Biana in New York.
651. KULINITE, 2AlSi2-fKSi2-l-3fi.
Crystalline, foliated. CI. along a prism of 135° 44'. G. ■=2-65.
Greenish grey, yellow, or brownish green. C. c. : 48 silica, 31 alumina,
2 '3 protoxide of iron, 6 '6 potash, 10 water. Killiney near Dublin.
652. Hygbophilite.
Scaly. H."2to2-5; G. =2'7. . Greenish grey. Lustre and feel
greasy. C.c: silica 48'4, alumina 32-1, protoxide of iron 3-3,
potash S 1, water 9. Sol in h. acid. Halle on the Saale.
653. Bkavaisite, R^Sij -f 2AlSi3 -I- 4fi .
Aggregatesof thin plates. H. = 1 to2; G. =2'6. C.c: silica 51 "4,
alumina 18-9, peroxide of iron 4, magnesia 3'3, potash 6-5, water
13-3. Noyant in Allier.
654. PlNITOID.
Massive. Leek- and oil. green. H. =2'5; G. = 2'8. Co. : silica
48 '5, alumina 28, protoxide of iron 8, potash 6 '8, water 4-5. Frei-
berg and Chemnitz in Saxony.
655. Bole.
Earthy, in nests and veins.. Conchoidal. H. = 1 to 2; G. =» 2 '2 to
2*5. Opat^ue ; dull resinous; streak shining. Brown, yellow, or
red. Feels greasy; some adhere strongly to the tongue, others not
stall. In water crackles and falls to pieces. C.c. hydrous silicates
of aluniiua and iron peroxide, in various proportions. Scotland,
Ireland, Dransfeld, Clennont in Auvergne. Slolpcnite, Rock Soap,
Plinthitc, Yellow Earth or Fclinite, Fdbol, and Ochran are varieties.
656. Carpholite, ilSi + ilnSi -f 2fi .
. Right prismatic Plll°27'. Radiating stellated. H. = 5 to 6-5;
G. = 2-9. Translucent; silky; straw- to wax-yellow. B.B. intuniesces
and fuses to an opaque brown glass. C.c. : silica 38, alumina 29-4,
protoxide of iron 2;9, peroxide of iron 4, protoxide of manganese
11-8, water 10-8. Schlaggeuwald, Wippra in the Harz, Meuville
b the Ardennes.
657. NONTEOKITE, ¥^'eSi3-f 6H.^
Massive; fracture uneven. H.-2 to 3; 6.-2 to 2'3.' Opaque;
dull or glimmering; streak resinous. Straw-yellow or siskin-green.
B. B. decrepitates, becomes black and magnetic, but without fusing;
sol. and gelatinizes in warm acids. C.c. : 43 silica, 36 iron peroxide,
and 21 water, with 3 '5 alumina and 2 magnesia. Nontion in
France, Harz, and Bavaria. CMoropal is similar,' E.B. brown.
Cnghvar in Hungary, and Passau.
658. PiNoniTE. _
Massive; fracture splintery; sectile. H. = l; G. = 2'3. Lightto
dark green. Lustre vitreous. Feels greasy. C.c. : Silica 36'9, per-
oxide of iron 29'5, protoxide of iron 61, water 25'1. \Volkenstein,
SuhL ~
659. HisiNGERITE, FejSi3-f2f'eSi-(-9fi.>
Reniform, and in crusts. H. —S'S to 4 ; G. =2'3 to S:w Opaque,
resinous. Brownish or bluish black; streak liver-brown or yellowish
brown. C.c: various, but 32'5 silica, 33*6 iron peroxide, 15'1
iron protoxide, and 19 water, in the Thraulite from Bodenmais,
Also Gilling and Riddarhyttan in Sweden, and Breitenbrimn
(Polyhydrile).
660. Eergholzi.
Fine fibrous; glimmering lustre. Wood-brown to green. G.=2'4.
C.c: silica 55 '5, peroxide of iron 19'6, magnesia 15, water lO'S.
Sterzing in Tyrol. Xylite, probably from the Urals, is similar.
661. UUBER.
Massive; fracture conchoidal. H. =1'5; G. — 2'2. Liver-brown;
streak shining. Mixtures of peroxide of iron, o^iidc of manganese,
and alumina with water. Cyprus. Hypoxanthite and Sidcrosili-
cite are similar.
162. Klipsteinite, (R3, SaJjSia-f R3H3.
Compact. H. —5 to 5'5; G. = 3"6. Liver-brown to black ; streak
yellow-brown. C.c: silica 25, peroxide of iron 4, sesouioxide of
manganese 57, water 9. Klapperud in Dalecarlia. Herbora near
Dillenburg.
663. Wglkonskoite.
Araoi-phous. Horny ; bluish green to grass-green. ' Fracture con-
choidal; brittle. C.c: silica 36, alumina 3, sesquioxide of chromium
19, ferric oxide 10, water 21. Okhansk in Siberia.
664. RiJTTISITE, 3NiSi-f4H.
Amorphous and reniform. Apple-green to emerald-green. H. = 2
to 2-5; G. = 2-35 to 2-37. C.c: silica 437, nickel oxide 35-0, water
11 '2. Rottis near Reichenbach in Saxony. KoviarU is similar.
665. Ubanophane, 3CaSi-ftJ'5Si3-l-18H.
Right prismatic. ooP 146°; ooPoo ; Poo; witb polar angle 60°.
Crystals honey-yellow ; when massive leek-green. H. «»2'5; G. «
2 '6 to 2 '8. C.c: silica 17, alumina 6'1, oxide of nraniuia 53'3,
lime 5"i, water 15'1. Kupferberg in Silesia.
666. Uranotile, CaSi-Htfa'Sij-HgH.
Right prismatic. coP 164. In stellate groups. Lembn.yellow.
G. = 3-96. C.c: silica 13-8, oxide of uranium 6675, liino 5-J7,
water 12'67. Wolsendcrf in Bavaria, Joachimsthal, Mitchel counly
in North Carolina.
667. BisMUTOFERBiTE, Bi, Sij, -f 2Fe,Si .
Crypto-crystalliue ; oblique prismatic Siskin- to olive-grccn.
H. =3-5; G. =4-48. C.c: silica 24, o-xide of bismuth 42'8, pevo-:ide
of iron 33 "1. Schneeberg in Saxony. Hypochlorite is a variety
containing 13 of bismuth. In a tlurd varietv. from Brannsdoif,
antimony replaces bismuth.
Silicates witu Titanates, Niobates, &c.
668. Sphene, (JaSij-fCaTij.
OHique prismatic, C 85° 22'. ooP (I) 133°2' ; JF"* {x) 55°
21';P"'a) (y)34°21'; ooP^oo (y) : 0P(i'or(;)90°; ooP«3 (i/) 76° 7' ;
P=« (r) 113° 30' ; §P=2 (n) 136° 12' ; 4P=4 (s) 67° 57'. Crystals
vary extremely in form, being generally ajipar-
ently oblique-tabular, from predominance of
71, which are hemidomes in alternate position
on opposite ends ; also,
but more rarely, pris-
matic, with dominance
of I and M. Twins fre-
quent. Twin face c,
and formed by revolution
either (a) on an axis nor-
mal to c or (6) on a vertical
axis ; the former very
common and usually pro-
ducing thin tables with
a re-entering angle alon(y"
one side, and sometimes
elongated. Occasionally
in double twins. Some-
times granular or foliated. ^ x-,, — . . . ,
to 5-5 : G. =3-4 to 3-6. Semitransparent ; adnmantiueorresiuousj
XVI. — 54-
Fig. 5S6. ^Fig. 687
CI. iiTsomc {I), in others (r). H.
426
MINERALOGY
Yellow, browB, and green. B. B. fuses with micro-salt in the red.
flame, gives reaction for titanic acid. C.c. : silica SO 6, titanic acid
40'8, lime 23 •&. In Scotland, typical of syenites and primary lime-
stones. In minute hair-brown crystals in the first; as at Lairg
.(Sutherland), Achavarasdale (Caithness), and Criffel (Kirkcud-
Fig. 688. Fig. 589.
bright) (figs. 636 to 58S). In the latter often in highly complex
twins, yellow to brown, at Shinness (figs. 193, 589), Urquhart,
Dalnain, Torbane, &c., also with ilmenite and allanite in exfiltra-
tion veins of grey granite. Dauphin^, Mont Blanc, St Gotthard,
Tyrol, Arendal, America. Grcniovite, flesh-red from Glen Gairn
in Aberdeenshire (like 194), and 3t Marcel in Piedmont; contains
manganese at the latter locality.
669. KEiiHAUiTE ( YttTotitanite), 5(CaY) (Sif i) -t- (KWe) (Sif 1)3 .
Oblique prismatic, C 53°. ooP 114. CL-2P, 138°. H. =6to
7 ; G. =3*6 to 37. Blackish brown ; streak greyish yellow. B.B.
■with borax fori^s blood-red glass in the red. flame ; other features
like sphene. C.c: 297 silica, 287 titanic acid, 21-1 lime, lO'S
yttria, 6*2 alumina, and 6 "5 iron peroxide. Near ArendaL
670. SoHORLOMiTE (Fen-o^i'/aitiVe), CajSi-FyejSij-J-CaTij.
Cubic ; raO and 202 ; generally massive ; fracture conchoidal.
H. — 7 to 7'5 ; G. — 3'8. tBlack ; streak grey-black ; vitreous. C.c.;
silica 26, titanic acid 23 '3, peroxide of iron 20, lime29'4. Arkansas,
ICaiserstuhl, Ivaara in Finland. Perhaos a titaniferous garnet.
671. TsOHEWklNITE.
Massive; fracture flat conchoidal. H. = 5 to 5 "5; G. = 4"5.
Opariue, vitreous, splendent. Velvet-black ; streak dark brown.
B.B. iutumcsces gieatly, becomes porous, and
often incandesces ; iu white heat fuses to black
glass ; gelatinizes with h. acid. C.c: 21 silica,
20 titanic acid, 11 iron protoxide, 45 peroxides
of cerium metals with jicrhaps thoria, lime 4.
Miask, Coromandel.
672. MOSANDEITE.
Oblique prismatic, C 71° 24J'. mP (<) 68°
36'; c»P''2 («); c»P»cD (a); -P (c) 124° 1';
-P°oo (j); ooP=oo. t: a 134° 18'; n : a 162°
62' ; q -.a 138° 2'. Twin face the orthopinacoid.
Generally massive. Fracture uneven. H. =4;
G. -2'93to3. Yellowish or reddish brown;
streak pale green. Vitreous to resinous lustre.
C.c. : silica 29 '9, titanic acid 9 ■9, oxide of cerium
metals 26-5, lime 19, water 8'9. Brcvig and
Langcsundfiord.
673. Ei'DiALiTE (JJiiWrte), 6RSi.-f SZr.
Khombohedj-al ; K 73° 10'. R (])), OR (aj, 00 P2 (<l{), JR (a^)
also t»R, JR, -*Ii. -2R. -iK. F-S, tP2
(fig. 691). Generally massive, granular.
CI. «! and rtg ; fracture uneven. H. = 5
to5'5; G. -2-84 to 2 -95. Peachblossom-
rcd to brownish red ; slreak white. Trans-
lucent; vitreous. B.B. fuses easily to a
light-green opaque glass ; gelatinizes iu
h. acid. C.c: silica 50, zirconia 16-9,
protoxide of iron 7, lime 11, soda 12.
Kangerdluai'suk in Greenland, Sedlova-
toi Island iu 'Wniito Sea, Brcvig {Eid-o-
lite). Magnet Cove in Arkansas.
674. CATAPLEITE,2(i*a.0a)(SiZr)p-f 9ft.
Hexagonal. P 1U° 48'. OP, ooP, P,
also with 2P, and JP. In lamellar aggro-
gates. CI. prismatic and P ; fracture
uneven. H. -6;G. -2'8. Yellowish br
yellow, lustrous. C.c: silica 467, zirconia 29'6, soda 108. water
9. Brcvig.
675. CErstedite.
Pyramidal. P 84° 25'. P, ooP, »P«. Like zircon. H.-5-5;
G. -303. Lustre adamantine Reddish brown. C.c: silica 197,
titanate of zirconia 08 -96, water 6 6. Arondal.
590 (sp. 672),
591 (sp. 673).
n to pale green ; streak
676. WoHUBEiTE, 9iiSi-H3RZr-(-{iS?b.
Oblique prismatic, C 70° 46'. ooP !
-P^to 43° 18'. OP : coP'oo 109°
15; -P°«> : "P'oo 136° 42' ;
OP : ooP 103° 31'. Crystals tabu-
lar and prismatic CI. clinodia-
gonal; fracture conchoidal. H. — 5
to6;G. -3-4. Light yellow, honey-
yellow to brownish grey ; streak
yellowish white. C.c: silica 28,
zirconia 19, niobic acid 13 "9, lime
27'8, soda 8'3, protoxide of iron
3. B.B. fuses to yellowish glass.
Sol. in h. acid. Langesundfiord.
677. Aedennite.
Right prismatic. mP 131° 2' ; Poo 112° 24'; H; »P| ; "f 2 ;
t>5p» ; mfto. Crystals like ilvanite. CI. brachydiagonal, and
t»P. H. -6 to7 ; G. ~3'62. Yellow to yellow-brown. Dichroic;
brittle. C.c. : silica 27 '8, alumina 24, protoxide of manganese 267,
lime 2'2, magnesia 4'3, vanadic acid 3'2, arsenic acid 6'3. water 5.
Ottrez in the Ardennes (Luxemburg).
678. ROSCOELITE.
Foliated masses, sometimes stellated. H. = 1; G. =<2'3 to 2'9.
Dark green to greenish bine. Pearly lustre. C.c; silica 477,
vanadic acid 22, alumina 14'1, magnesia 2 potash 7'6, water 5.
Eldorado iu California.
TITANATES 'WITH NIOBATES.
679. TiTAKOMOEPHITE, CaTi,.
Oblique prismatic. Like sphene. 00 P, OP, 5P°«J, P°<»,
IV^2. C.c: titanic aciri 74*3 lime 25*3. Lampersdorf in Silesia,
iVeistiitz.
680. Peeovskite, CaTi .
Right prismatic. In complicated twins, often distorted, pseudo-
cubic. H. — 5'5; G. =4to4'l. Lustremetallic-
adamantine. Pale yellow, reddish brown to
iron-black; streak grey. C.c: 58*8 titanic
acid, 41 '2 lime. B.B. with micro-salt in outer
flame gives a bead greenish while hot, colour-
less on cooling; in inner flame grey-green
when hot, violet-blue when cold. Decomposed
by boiling s. acid. Zlatoust, Schelingen, Zer-
matt, Malenco Valley near Sondrio, Plitsch
in Tyrol, Magnet Cove in Arkansas.
681. KoppiTE, RjNb. .
Cubic; ooOrn. G. -4'45 to 4-56. Brown. Transrarent. C.c:
niobic acid 62'46, oxide of cerium 6 7, oxide of lanthanum 3.
Schelingen on the Kaiserstuhl in Baden.
632. AxSERoDiiE, 2RjJfb-h5S:
r.ight prismatic. H = 6. G 6 7. Mcte.llic to greasy. Black.
Streak black, brown, greenish grey. Translucent in splinters;
brittle. C.c: 48 niobic acid, with zirconia, thoria, ceria, yttria,
and uranium o.xide. Annerbd near Moss 'Norway).
683. DysAnaltte, eR'Ti-hRJib.
Cubic; mOoo. CI. cubic. G. -4-13. Black. C.c: titanic acid
41 '5, niobic acid 23 2, cerium oxide 57, lime 19 '8; protoxide cl
iron 5 "8, soda 3*6. Vogtsburg on the Kaisenstuhl.
634. PruocHLOHE, 5RJfb-h4ii(Ti'ifh)5-l-4NaF.
Cubic (fig. 694). Cl. oclaliedral ; brittle ; fractnre conchoidal.
H. -5; G. -4 -2 to 4-4. Resinous,
opaque. Red-brown to black, ruby-
red and transparent rarely; streak
pale brown. C.c: niobic acid
53-2, titanic acid 10-5, thoria 7'6,
cerium oxide 7, lime 14 '2, soda
5, fluorine 3 1. Miask, Kaiser-
stuhl, Brovig, and Fjoderiksvarn.
Microlitc, from Chesterfield in
Massachusetts, has tnntalic acid
C8'4,- niobic acid 776, 1 17 lime
and 77 protoxide of manganese.
I'linhitc from JIursinsk in the
Urals, San Picro in Elba, and tho
Azores may be the same ; at tlie
last locality it is in orange-red
oct.ahedra, and is a uiobatc of zirconia.
GS5. Elomstbasditb, (Ca,Fe), Ti-^^jrjfbJ-^^^.
.Missive. U.-6-5. G. -417 to 4-25. Vitreous, block. Etreait
.594.
MINERALOGY
427
^oiRi. "Rjuulocent in iplinters." C.c. : niobic ecid 49-8, titanic
Boid 107, onnium oxide 237, protoxide of iron 3-3, lime 8'6,
water 7-D. NoU (Sweden); ^f
886. POLTOEAaB, 4BTi + Mb.
Bigbt jnlsmatic (fig. 695). oof is , ooP
(140°), P, 2P«J (66°). Fracture coHchoidal.
H. -6 to 6 ; 0.-5-1. Black ; atreak grey-
brown. 6.B. decrepitates violently, incan*
descing, but does not fuse. Sol. in «. acid.
Co.: titanic acid 26 fi, niobic acid 20-4, yttria
23-3, erbia 7'5, oxide of uranium 77, water
4. Hittero (Norway). Slettikra in Jonkop-
ing (Sweden).
587. EincENiTE, 2RiH+Mb + fi.
Eight prismatic (6g. 696). ooP (m) 140°f
oof oo (6) ; 2P00 (d) 62" ; P (p\ 102° 68'.
p : 6 103° 6'. Fracture conchoidaL Opaque ;
metallic to vitreous. Black and brownish
black; streak red-brown. B. B. infusible. Not
acted on by acids. C.c. i niobic acid 32,
titanic acid 19 '2, uranium oxide 19 '5, yttria
18 '2, cerium oxide 2 '8, but variable.
Jblster, Tromo, Alvo, ic, in Norway ; also
Hittero and Cape lindesnaes.
688. .AsOHTKiTE. Fig. 596.
Bight priamatic ooP (If) 128' 34'; 2?oo (y) 73° 16' ; P (0 : 0)
137° 14'; ooP3 69* 23'; Poo ; OP. Crystals long prismatic (fig.
697). CL traces ; fracture imperfect conchoidal. ^r^
H.-6to6-5; G.-4-9 to 5-1. Opaque ; submatallio /v\\
or resinous. Iron-blick or brown ; streak yellow- /^4-"V'\
ish brown. B.B. swells and becomes yellow or
brown, but is infusible. Kot sol. in h. acid,
partially in s. acid. C.c: niobic and t°nCalic acids
28 -8, titanic acid 22 '6, thorium oxide 15'7, cirtam
protoxide 185, lanthanum oxide and didymiam
oxide 6 '6. Kiask, Hittero.
689. PoLYMIONITB. ■
Right prismatic P (p) polar 136' 28' and 116°
W ; ooP 109° 46' ; ooPaj ;
oof 00 (fig. 698). Cn. macro-
and brachydiagonal, imper-
fect ; fracture conchoidaL H. — 6 '5 ; Q. —
4*7 to 4-8. Opaque; semixoetallic Iron-
black ; stt-eak dark brovsa. B.B. infusible.
Sol. inh. acid. C.c: titanic acid 46 3, zir-
conia 14-1, yttria ll-5,ltme 4-1, iron peroxide
12-4, cerium ox-
ide 6. Frederiks-
vUm.
690. Menqite,
(^, Zr)*!.
Right prisma-
ti*." : P(«) polar angle 151° 27' and 101°
IC; >»P186°20'; oofS; ooPoo (fig. 699X.
Fracture uneven, H. — 5 to 5-5; O. —
5-48. Opaque ; semimetallic. Iron-
black ; dtreik chestnut-brown. B. B.
infusible, but becomes maf^etio. Sol.
in 8. acid. Miask, Groix island in Uorbihan.
891. Tantalite, ie (¥a, jSb).
Right prismatic. P (p) with polar edges 126° and 112° 30',
middle 91° 4^. . aff (r) 122° 63 • oopoo (s);
oof 00 ((); f» (m) US' 48; 3f<» (q) 54°
IC; if 00 (n) 167° 36'; fPj (r) ; 2P2 (0).
Fracture coacholdal or uneven, H. — 6 to
6-6;G. -ei to 8. Opaque; semimetallic,
adamantine, or resinous. Iron-black ; streak
cinnamon- or coffee-brown. B.B. infusible ;
scarcely affected by acids. Cc. : 76 to 50 tan-
talic acid, 7 '5 to 29 niobic acid, 9 to 16 iron
protoxide, and 1 to 6 manganese protoxide ; some with 1 to 10 tin
oxide {Casaiterotantalite) ; also in union with iron (manganese)
ytotoxide. Kimito and Tammela in Finland, Broddbo and Finbo
near Falun, and Chanteloube near Limoges ; alwaja in granite.
692. Tapiolite, 4fe¥a + f'eKb.
Pyramidal P middle angle 84* 62', summit 123°!'. H.-6;-G.-
Fig. 697
(sp, 638).
/Fig. 698 («p. 689),
Fig. eeO (sp,
Fig. 600.
7-2 to 7-6. Black. Lustrous. C.c: tantalic acid 78-9, niobic acid
11-2, protoxide of iron 16. Tammela in Finland.
693. CoLxriCBITE, mtejifb -mf^ia .
Right prismatic. P («) polar angles 104° 10" and 161', middle
angle 83' 8'; OP (c); ooPoo (J); ooF<o (a); o=P (j) 136' 40';
ooi-oo (m) 101' 26'; 2P (») ; 3!'3 (0); 3fi (w) ; Jpco (!) lei'i;
?«. (t) 143° ; 2f 00 (A) 112° 26' ; Poo (f) 101' 12' ; 2Pa! («) 62° 40'.
Hemitropes, face e ; vertical axes forming an angle of 62° 40' ; also
on faces 2P2 (n), and rarely b. Also granular and foliated.' CL
brachydiagonal, perfect, also macrodiagonal. H. — 6 ; G. — 6-4 to
6 4. Metallic, adamantine. Iron-black to brownish ; streak blade
ZSEZZv
'isiiL-^
Fig. 603.
Fig. 601. Fig. 602.
or reddish brown. B.B. infiwihle ; not affected by acids. CcH
isomorphic mixtures of niobic and tantalic acids with protoxide of
iron (or manganese). Pure columbite would give 78-8 niobic acid,
pure tantalite 86 tantalic acid. The niobic acid generally prevails,
and the crystals are better formed the more this is the case.
Rabenstein, Bodenmais, Chanteloube, Finland, Ilmen Hills,
Evigtok in Greenland, Haddam and Middletown in Connecticut,
Acworth in New Hampshirs, Pike's Peak in Colorado.
694. Ytthotantalite, (Y, Ca, Fe, tl)j(*a, W, Nb).
In two varieties, (n) BlacH. Eight prismatic ; in short pris-
matic or tabular crystals, oofoo ; ooP (m) 121° 48'. OP : 2? 00
103° 26' ; p!o : OP 131° 26'; » : i 140'
42' (fig. 604) ; also in grains aud lamellee.
CL brachydiagonal, indistinct; fracture
conchoidal or uneven. Opaque, or in thin
splinters translucent. Velvet-black, semi*
metallic lustre, and greenish grey streak.
H.-5-5; G. -5-4 to 57, (b) Yelloio.
Amorphous, yellowish brown, or yellow,
often striped or spotted ; resinous or vitre-
ous ; streak white. G. -5-46 to 6-88.
Both varieties B.B. infusible, but become „. g^.
brown or yellow. Not affected by acids. '8- " •
C.c: 67 to 60 tantalic acid, 1 to 8 tungstic acid, 0 to 20 niobic
acid, 29 to aS yttria, 0 5 to 6 lime, 0-6 to 6 uranium peroxide,
and 0-6 to 3-5 iron. peroxide. Ytterby, and near Falun.
695. Ferousonite, (Y, Er, (5e)3(i!fb, ¥a).
Pyiemidal and hemihedric ; P (5) 128° 28'. Usual form (i) 3P|
(j), P, J 00 Pi (y). OP (c) (fig, 605), *:» 100'
54', f.c 115' 16', s: r 169^ 17. CI. traces
along P; fracture imperfect conchoidal; brittle.
H,-5-6 to 6; G. -5-6 to 6-9. Translucent
in thin splinters ; semimetallic. Brownish
black; streak pale brown. B.B. infusible. ,
C.c: chiefly niobic acid and yttria, with erbia, 1
also a little cerium protoxide, tin oxide, ura-
nium oxide, and iron protoxide. Cape Fare-
well in Greenland, Ytterby, Riesengebirge,
Rockportin Massachusetts. Tyrilt, from Helle
near Arendal, is similar.
696. Hjblmite,
Massive, with granular fracture and traces
of erystala. H, -6; G, -6-82. Velvet-black;
black. Lustre metallic. Cc, : tantalic acid 62-4, tin 6 6, uranium
4-9, protoxide of iron 8-1, yttria 6-2, B,B, infusible. In closed
tube decrepitates and yields water. Kararfvet near Falun.
697. Samabskite (UranotantaliU), (fl3,R,R5),^*a)3.
Right prismatic ooP 122° 46'; o=f 2 96°; Poo 93°; P; oopoo ;
ooPoo ; 3pJ ; also in grains. Fracture conchoidal ; brittle, H. -
6-56; G. — 5-6 to 6-76. Opaque; strong semimetallic. Velvet-
black ; streak dark reddish brown. B.B. fuses on the edges to a
black glass. In the closed tube decrepitates, yields water, incan-
desces, and becomes browi, Sol. in h. acid to a greenish fluid.
428
MINERALOGY
C.c. : 37'J niobic acid, 18'6 tantalic acid, 12 iron protoxide, 14 to
20 uranium oxide, 6 thorium oxide, 4 zirconia, and 16 yttria with
lime and magnesia, filiask, Mitchell county in North Carolina.^
The YUroiLncnile of Hermann.
C98. NoHLiTE, RjNb.
Massive. H-4-5to5; G. =5-04. Black-brown. Splintery.'
Brittle. Opaque; vitreous. Niobic acid 50'4, uranium oxido 14-4,
2irconia 3, ferrous oxide 8, yttria 14'4, lime 47, water 4-6. Nohl
near Kongelf (Sweden).
699. Hatchettolite.
Cubic; 0, ooOoo. Yellowish brown. Resinous lustre. Frac-
ture conchoidal. H. -5; G. -4-8 to 4-9. C.c: niobic acid 34-3,
tantalic acid 29'8, uranium oxide 15-5, lime 8-9, water 4'6. North
Carolina.
ANTIMONUTES.
700. RoMEiTE, CajS'bSb .
Pyramidal; P 110° 50'. Scratches glass. G. =47. 'Honey-yellow
or hyacinth-red. B.B. fuses to a blackish slag. Sol. in acids.
C.c. : 41-3 antimonic acid, 37-3 antimony oxide, and 21-4 lime, but
with 2 to 3 manganese and iron proto.xide. St Marcel in Piedmont.
Schnccbcrgite, from Tyrol, may be an impure variety.
701. Blelniere, fb^Sb, 8b) + H .
Eeniform and massive. H. = 4 ; G. = 3 -9 to 4 '8. Translucent ;
resinous to earthy. Colourless, yellow, brown, and grey. B.B.
reduced on charcoal. C.c; oxide of lead 41 to 62, antimonious
acid 32 to 47,. water 6 to 12. Lostmthiel, Horhausen, Nertcliinsk.
702. Nadokite, PbSb-HPbClj.
Eight prismatic ; ooP 132° 51'. Crystals tabular. CL macro-
diagonal. H. — 3; G. =7. Yellowish or greyish brown. Resinous
to ad.imantine ; translucent. C.c: lead 52*2, antimony 30 '8,
o-\'ygen 8, chlorine 9. Constantino (Algeria).
703. ElVOTlTE.
Massive. Yellowish to gre}'ish green. Opaque ; fracture un-
even ; brittle. H. -3-5 to 4; G. -3-6. C.c: oxide of copper
39-6, oxide of silver 1'2, antimonic acid 42, carbonic acid 21.
Sierra del Cadi in the province of Lerida. Thrmnholiic from Rez-
banya, Hungary, may be a hydrated variety.
704. Mellite, Al(Ci20s) + 18H.
Pyramidal ; P 93° 5'. OP; Poo; and coPco
conchoidal ; brittle. H.- 2 to 2-5; G. -=l-5to
1"6. Transparent; doubly refractive; vitre-
ous. Honey-yellow or reddish ; streak white.
In closed tube yields water. B.B. chars with-
out odour. Burns white and acts like alumina.
Sol. in n. acid or potash. C.c. : alumina 14-4,
mellic acid 40-3, water 45-3. In lignite at Fig. 606.
Artern in Thuringia and Luschitz in Bohemia; Walchow in
Moravia (cretaceous); in coal at Malovka iu Tida.
705. Ox.ALiTE, 2Fee3 + 3a.
Capillary crystals, also botryoidal or compact ; fracture uneven ;
H. — 2;G.=2-2. Opaque; resinous to dull. Straw-yellow,
to yellow solution in acids. C.c:
acid, 15 '8 water. In lignite at
and Gross Almei'ode in H esse.
CI. P ; fracture
sectLli
B.B. turns black, then red
42-1 iron proto.xide, 42-1 oxal:
Kolosoruk near Bilin, Duisburg
706. Whewellite, Ca'e + H
Oblique prismatic, C 72° 41',
brittle H. -2-6 to 2-8; G.^
vitreous. Colourless.
water. Hungary.
ojP 100° 36'. CI. basal, perfect;
■1*838. Transparent to opaque;
C.c: 49-31 oxalic acid, 38-36 lime, 12-33
THE MINERAL RESINS.
Many of these are only vegetable resins slightly altered. Naphtha
is fluid ; the others solid, with H. -1 to 2 or 2-5. Most are amor-
phous, a few crystalline and monocliuic G. -0-6 to 1 -6. Mostly
resinous ; colourless, or coloured brown, yellow, or red, with paler
streak. Sol. in acids, alcohol, ether, and oUs. Melt readily, and
bum with fiamo and smoke.
707. NArHTHA, Petholeum, CH„.
Liquid. Colourless, yellow, or brown. Transparent or translu-
cent. G. -0-7 to 0-9. Volatilizes in the atmosphere with an
aromatic bituminous odour. C.c: 84 to 88 carbon, aud 12 to 16
hydrogen. Varieties are —
Knphtha. — Very fluid, transparent, and light yellow. Tegern
Lake iu Bavaria, Amiano near Parma, Salics in the Pyrenees,
Rangoon, Baku on the Caspian Sea, China, Persia, and North
America. Used for burning, and in prej^aring vnroislies.
Petroleum. — Darker yellow or blackish brown ; less fluid or
Tolatile. . Ormskirk in Lancoshiro ; Coalbrookdale, PitcUfoid, and
Madeley in Shropshire ; St Catherine's "Well, south of Edinburgh ;
Mainland of Orkney ; and many other parts of Europe.
708. Elaterite {Elastic Bitumen, Mineral Caoutchcuc)^ C^ .
Compact ; reniforra or fungoid ; elastic and flexible like caout-
"chouc, very soft. G. = 0 -8 to 1 '23. Resinous. Blackish, reddish,
or yellowish brown. Strong bituminous odour. C.c: 84 to 86
carbon, 12 to 14 hydrogen, aud a little oxygen. Derbyshire,
Montrelais near Nantes, aud Woodbury in Connecticut./
709. Asphaltum, Bitumen.
Compact and disseminated ; fractui-e conchoidal,''Bometimes
vesicular; sectile. H. — 2; G. — 1-1 to 1-2. Opaque, resinous,
and pitch-black; strong bituminous odour, especially when rubbed.
Takes iire easily, and burns with a bright flame and thick smoke.
Sol in ether, except a small remainder, which is dissolved in oil
of turpentine. C.c: 76 to 88 carbon, 2 to 10 oxygen, 6 to 10
hydrogen, and 1 to 3 nitrogen. Limmer near Hanover, Seyssel on
the Rhone, Val Travers in Neufchatel, Lobsann in Ahsace, in the
Harz, Dead Sea, Persia, and Trinidad ; Cornwall, Haughmond Hill
(Shropshire), East and West Lothians, Elie and Burntisland (Fife).
710. Albe:.tite.
Massive. Velvet-black. Adamantine lustre; brittleT^s'C.c.:
carbon 86, hydrogen 9, nitrogen 2-9, oxygen 2. Hoy, Orkney;
Sti-athpefl'er, Ross ; Hillsborough, New Brunswick.
711. PlACZITE.
Massive; imperfect conchoidal, sectile." H. =1-5; C. = 1'22.
Dimly translucent on very thin edges ; resinous. Blackish brown ;
streak yellowish brown. Fuses at 600° Fahr., and burns with an
aromatic odour, lively flame, and dense smoke. Sol. in ether and
caustic potash. Piauze near Rudolfswerth in Carniola.
712. IXOLYTE.
M.assive ; conchoidal fracture. H. — 7; G.— 1-008. Resinous.
Hyacinth-red ; streak ochre-yellow. Rubbed between the fingers
it emits an aromatic odour ; becomes soft at 119°, but is still
viscid at 212°. Oberhart near Gloggnitz in Austria,
713. AiiBER {Succinite), CjoHjO.
Round irregular lumps, grains, or dpps. Fracture Twrfect con-
choidal; slightly brittle. H.-2to2-5 ; G.-l tol-1. Transparent
to translucent or almost opaque; resinous. Honey-yellow, hyacinth-
red, brown, yellowish white ; also streaked or spotted. When
rubbed emits an agreeable odour, and becomes negatively electilc
It melts at 550°, emitting water, an empyreumatic oil, and. succinic
acid ; it burns with a blight flame and pleasant odour, leaviug a
carbonaceous remainder ; only a small part is soluble iu alcohoh
C.c : 79 c.Ti-bon, 10-5 hydrogen, and 10*5 oxygen. Derived chiefly
from an extinct coniferous tree {Pittites succini/cr), and found
in the Terti.aiy and diluvial formations of many countries, especially
northern Germany and shores of the Baltic, Sicily, Spain, and
northei-n Italy, rarely in Britain (on the shores of Fife, Norfolk,
Suffolk, and Essex, and at Kensington, near London). Used for
ornamental purposes, and for preparing succinic acitl and var-
nishes. Krantzitc, from Nienburg, is essentially the same.
714. Retinite {Sctinasphalt).
Roundish or irregular lumps ; fracture uneven or conchoidal ;
very easily frangible H. -1-5 to 2 ; G.-l -05 to 1-15. Trans-
lucent or opaque; resinous or glistening. Yellow or brown. Melts
at a low heat, and burns with an aromatic or bituminous odour.
C.c: in geuei-al carbon, hjdrogcn, and oxygen, in very un-
certain amount. Bovey, Halle, Cape Sable, aud Osnabriick.
Pyrorctinitc from Aussig in Bohemia is similar.
715. Walcuowite, C^Mfi .
Rounded pieces, with a conchoid.il fracture. H. = 1-5 to 2;
G.-l 035 to 1-009. Tianslucent, resinous. Yellow with brown
stripes, and a yellowish white streak. It fuses at 482^, and burns
readily. Soluble partially (7 -5 per cent. ) in ether ; in s. acid forms
a dark-brown solution. C.c: SO-4 carbon, lO"? hydi-ogcn, and
8-9 0X3-gen. Walcliow iu Sloravia.
716. CoPALiXE {Fcssil Copal, Eiohrjalc Ecsiii), Cj^HcjO.
Inegularfragments. H. - 1 -5; C. - 1 -046. Traiisliu-cnt, resinous;
burns i\ith light yello\\' flame and much smoke; alcohol dissolves
little of it; becomes black iu suljihuric acid. C.c: 85-54 carbon,
11-63 hydrogen, 2-76 oxygen. Highgate near London. .V similar
resin from Settling-Stones mine iu Nortluimberhmd, found iu Hat
drojis or crusts on calc-spar, is infusible at 500° Fahr. ; G. — 1 -16 to
1-54; it contains 86-13 carbon, 1085 hydrogen, aud 3-26 ashes.
717. Behexoelite, CjjHjjOj.
Amorphous; conchoidal fracture. Dai-k brown, inclining to
green; yellow .■streak. Resinous; uupleasaut odour, ami bitter
tasto. Fuses below 212°. ami continues soft afterwaixls i>t oiilinary
temperatures; easily soluble in alcoliol. Co.; 72-40 carbon, 9-y8-
hydrogen, 18-31 oxygeu. Sail Juan do Bercngela in Peru.
718. GrAYAQflLLITE, C.oH„Oj.
Amorphous ; yielding easily to thi: knife, and very friable. G.
M I H E R A L 0 G Y
429
— I'OOS. Pale yellow. Slightly resinous. Fluid at 21 2^ viscid
when cold; slightly soluble in water, and largely in alcohol, forming
a yellow fluid with a bitter taste. C.c. : 77*01 carbon, 8*18 hydro-
gen, and 14*80 oxygen. Guayaquil in South America.
Soghutter, from the Irish peat mosses, is similar ; it melts at
124", is easily soluble in alcohol, and contains 73'70 carbon, 1260
hydrogen, and 13*72 oxygen.
719. Hartine, CsoHjd+H.
Round masses or thin layers. Brittle, but easily cut with a
knife. G, = 1 '6. Resinous. Reddish brown by reflected and deep
red by transmitted light ; streak light brown. Becomes black on
exposure. C.c: 86'43 carbon, 8*01 hydrogen, 5'56 oxygen. In
the main coal seam at Middleton near Leeds, and at Newcastle.
720. Ozocerite {Native Paraffin), CH .
Amorphous, sometimes fibrous. Very soft, pliable, and easily
fashioned with the fingers. G. =0'94 to 0"97. Glimmering or
glistening; semitransluceut Yellowish brown or hyacinth-red by
transmitted, dark leek-green by reflected light. Strong paraffin
or aromatic odour ; fuses easily to a clear oily fluid ; at higher
temperature burns with a clear flame, seldom leaving any ashes ;
readily soluble in oil of turpentine, with great difficulty in alcohol
or ether. C.c: 857 carbon, and 14'3 hydrogen. Binny (Linlith-
gow), and Edinburgh ; Slanik and Zietriska in Moldavia, near
Gaming in Austria, and Baku ; also at Urpeth coal-mine near
Newcastle-ou-Tyne. PyropUsitc may be a variety.
721. Hatchettine {Mineral Tallow).
Flaky, like spermaceti; or subgranular, like beeswax; soft and
flexible G. =0-0. Translucent; weak pearly. Yellowish white,
wax-yellow, or greenish ycllov;. Greasy inodorous; readily soluble
in ether. C. c. : 85 91 carbon, 14 "62 hydrogen, or similar to ozocerite.
Loch Fyne (fusible at 115°), Merthyr-Tydvil, Schaumburg,
722. FiCHTELITE, C4H3.
Crystalline (oblir^ue prismatic) lamellje, which swim in water,
but sink in alcohol. Wliite and pearly. Fuse at 114°, but again
become crystalline on cooling. Very easily soluble in ether, and pre-
cipitated by alcohol. C.c. : 88 '9 carbon and 11 1 hydrogen. In pine
wood in a peat-moss near Redwitz in Bavaria.
723. Hartite, CqHjj.
Anorthic; but mostly like spermaceti or white wax, and lamellar.
Sectile, but not flexible. II. =1; G. -1-046. Translucent; dull
resinous. "White. Melts at 165", and burns with much smoke.
Very soluble in ether, much less so in alcohol. C.c; 87'8 carbon,
and 12-2 hydrogen. Oberhart in Austria.
724. KoNLiTE, C^H.
Crystalline folia and grains. Soft. G. = 0-8S. Translucent;
resinous. "White, without smell. Fuses at 120° to 137°. Sol. in
n. acid; precipitated by water in a white crystalline mass. C.c:
92 3 carbon, 7*7 hydrogen. Uznach near St Gall, Redwitz.
725. Scmi;ei:erite, CHj,
Oblique prismatic ; tabular or acicular. Soft and rather brittle.
G. = 1 to 1"2. Tran.<;lucent; resinous or adamantine. White, in-
clining to yellow or gi-een. Feels greasy, has no taste, and when
cold no smell, but when heated a weak aromatic odour. Insoluble
in water; readily sol. in alcohol, ether, and n. and s. acids. C.c:
75 carbon, 25 hydrogen. Uznach. Branchite, white, translucent,
fusing at 167°, is similar; Montevaso in Tuscany,
726. Idrialite, C3H2.
Massive; fracture uneven 0X slaty; sectile. H. = 1 to I'S;
G. = l-4 to 1'6 (17 to 3'2). Opaque; resinous. Greyish or
brownish black ; streak blackish brown, inclining to red. Feels
greasy. Burns with a thick smoky flame, giving out sulphurous
acid, ami leaving some reddish brov.n ashes. C.c: 77 idrialine
( = 94-7 carbon and 53 hydrogen) and 18 cinnabar, with a little
silica, alumina, pyrite, and lime. The idrialitic may be extracted
by warm olive oil or oil of turpentine as a pearly shining mass,
difficultly fusible. Idria. I
727. TORBANITE.
Massive ; fracture subconchoidaL Yellow, brown-grey, and light
brown. H. = 15 to 2; G.-1-28. C.c : 60 to 65 carbon, 9 hydrogen,
4 to 5 oxygen, 10 to 20 silicate of alumina. When distilled below
redness yields a burning fluid holding paraffin in solution ; above
redness a large quantity of highly Uluminating gas. Shown by
the microscope to consist of granules of a yellow bituminoid wax,
vrith interstitial shaly matter. Torbanehill iu Scotland. Pilsen
in Bohemia, Eurakina and Murayevna in Russia.
728. DOPPLERITE.
Jelly-like elastic masses. Brownish black ; streak browia. Greasy
lustre H. =0-5; G. =1-1. After drying H.-2-5; G. = 1*5. Insol-
uble in alcohol and ether. An acid substance related to humic
acid. From peat beds, Auasee (Styria) and Switzerland.
THE COALS.
729. Anthracite {Glance Coal).
Massiveanddisseininated; rarely columnar. Fracture conchoidal;
brittle. H.=2to2-5; G. = 1 '4 to 1 7. Opaque; brilliant metallic
Iron-black; streak unaltered. Perfect conductor of electricity.
Burns difficultly with a very weak or no flame, and dots not cake ;
in the closed tube yields a little moisture, but no crapyreumatic
oil ; detonates with nitre. C.c: carbon above 90 per cent., with
1 to 3 oxygen, 1 to 4 hj'drogen, and 0 to 3 nitrogen; and ashfts
chiefly of silica, alumina, lime, and peroxide of iron. Common iu
some parts of all coal-fields; and especially in the United States, as
in Rhode Island, Massachusetts, and above all in Pennsylvania.
Used chiefly for manufacturing metals.
730. Common Coal {Black Coal, Stone or Mineral Coal, Bitu
minous Coal).
Compact, slaty, or confusedly fibrous; often dividing into rlioin-
boidal, columnar, or cubical fragments. Fracture conchoidal, nii-
even, or fibrous; rather brittle or sectile. H. -= 2 to 2 '5; G. = 1 '2 to
1*5. Vitreous, resinous, or silky in the fibrous variety. Blackish
brown, pitch-black, or velvet-black. Burns easily, emitting flamo
and smoke, with a bituminous odour ; heated in the closed tube
yields much oil. C.c : 74 to 90 carbon, with 0*6 to 8 or 15 oxygen,
3 to 6 hydrogen, 0 to 1 to 2 nitrogen, O'l to 3 sulphur, and 1 to 11
earthy matters or ash, in 100 parts.
Slate Coal QvSjilinthns a. thick slaty structure, and an unevett
fracture. Clicrry Coal is the name applied to the brittle highly lus-
trous variety common in the English coal-fields. Caking Coal is a
more bituminous variety which undergoes semifusion when ignited,
caking or agglutinating during combustion. Cannel Coal has a resin-
ous, glimmering lustre, and a flat-conchoidnl fracture, breaks into
irregular cubical fragments, but is more solid and takes a higher
polish than other varieties. This burns with a bright flame, and
yields much gas. Abundant in many lands, as in England, Scot-
land, and Ireland, in Belgium and France, in Germany and
southern Russia. British America and the United States possess
ininieuse fields, especially in the valley of the Mississippi. Also
found in China, Japan, Hindustan, Australia, Borneo, and several of
the Indian islands.
731. Lignite {Jety Brovm Coal). ^
Distinctly vegetable in origin, — the external form, and very often
the internal woody structure, being preserved. The texture is com-
pact, woody, or earthy. Fracture conchoidal, woody, or uneven ;
soft and often friable. G. = 0'5 to 1"5. Lustre sometimes resin-
ous, mostly glimmering or dull. Brown, black, or rarely grey.
Burns easily with an unpleasant odour; colours solution of potash
deep brown. C.c: 47 to 73 carbon, 2-5 to 7-5 hydrogen, 8 to 33
oxygen (with nitrogen), and 1 to 15 ashes. Jet is pitch-black, with
conchoidal fracture and resinous lustre. Brown coal occurs at
Bovey-Tracy in Devonshire; also in Germany, Hungary, France,
Italy, and Greece. Tho Surturbrand of Iceland seems a variety.
Used as fuel, but much inferior to common coal. The Oolitic
coals of Yorkshire, Antrim, Brora, Mull, and Skyc are intermedi-
ate varieties.
Index of Mineral Species.
Abiiachnnltc, £81.
Acnnfhlte, 170.
Acmltc, 570.
Actinolitc. 578.
Adamite, 410.
Adlnole, 590.
Adulnrlii. 5S9.
vERcrinc, 671.
>EscIiyiaie,.CS3.
llllunite. 231.
Alnbandlnc. 180.
Alabnsttr, Sll*.
Alalitc. 6C7.
AJbertltc 710.
Albite. 000.
Alexondi'ite, 94.
AlKodon4ie, 192.
Allanitc, 474.
Allumontlte, 7.
Alloclivuitc, 493.
AUonioniliite, 313.
AUopiilUdUini, 30.
AUftiilumc, Ca9. ■
Almiindine, 493.
Alstonlte, 283.
AlUite, IG3.
Alu
. 341.
Alonogenc, 328.
Amolgam, 24.
Amazon stone, 389.
Amber. 713.
Amblyconitc, 450.
Ainbljstcgitc, 5G5.
Amethyst, 81, 135.
Amianthus, 567,
578.
Amphlbolc, 673.
AmvhodcUtc, 591,
.\na1chnc, CO-j.
Anutasc, 9C.
Anatixito, C41. i
Andulu3itc 4C0.
Andcsinc, 594.
AnglcsUc, 31C.
Anhydi-Uc, 312.
Aniccritc, 274.
AnmiborKitc, 338.
Annerudttc,C82.
Anntdte, 233.
Anomitc, 515.
Anoi-thite. 691.
Anthoiihyllite, 517.
Anthracite, 729.
Ant Ill-aconite. 272.
Antigoilte, 5-31.
AntimonUI nickel,
184.
Antimony, 6.
Apatclite, 331.
Apatite, 443.
Aphi-ite. 272.
Aphiodire, 545.
j Apophyllitc, C03.
Aqnam.iriiio. C3G.
Arngorita, 281.
Arcuiiltc, 308.
Ardcnnite, C77.
Arfvcdannite, 579.
Arscniite. Ifi9.
Ark.inaite, 97.
Aiksutite, 41.
I Aiquerite, 23.
Arsenic, G.
ArseniosldcrUe,429.
Arscnoiite, 123.
Asbestos, 673.
Asphaltum, 709.
Astrukanitc, 337.
AstrophyUire, 630.
I Atncamite, C9.
Atopite, 37G.
1 Augitc, 507.
Aiii-ichiilcite, 397.
; Avaltc. 28.
: Ava
, 135.
Dabingtonlte, 575*
liaikalito. 5G7.
Bni-sovlte, 596.
Uaryta-mica, 521.
Barytc, 313.
Baiyto-calcito, 287.
Barjto-celestlne,
- 314.
Brtstite, 564.
Btlstiiacslte, 37.
neaumontite, 614.
Beauxltc, 112.
Beegcrite. iCO.
Deraunitc. 400.
Bcrenselite, 717.
Bergholz, cr.0.
Beilhlciinc, SG
Berthierlte, 2H'
Beryl, 5SC '
Berzellnlte. t6(
Bcrzelite, 370.
Beiidintite, 45':.
Bicberlte, 327.
Dlnnlte, 221. '
Biotite, 512.
Blsmltc. 126.
Bismuth, 8. '
Bismutliine. 209r
Blsmuthlte, 302.
I)i8inuto(enlta.C^
430
Blsmnto-spbcrite,
288.
Bitt«r-spftr, 373.
Bitnraen, 708. 709.
Blelolere. 701.
Blende, 177.
Wbdlte, •337.
Blomstrandlte, 685.
Bloodstone. 13&.
Bodenite, 474.
BoRbutter, 718.
Bogo&lovsklte, 492.
Bole, 655.
BoUTite, 256.
BoIo(nieso stone,
313.
BoltoQite, 476.
BoDsdorflte, 665.
Boraclte, 262.
Borax. 266.
Bomite, 190.
BorocalcUe, 267.
Botiyogenc. 347.
BotryoUte. 470.
Boulangerite, 227.
Bounionlte, 230.
Branchite. 726.
Brandisite. 524.
Bi-aunite. 100.
Bravalsite, 653.
Breislackite, 567.
Breithauptite, 184.
Breiinnerite, 276.
Brewsterite, 615.
Brochantite, 334.
Bromlte, 56.
Brongniailine, 311.
Bronzite, 564,
Brooklte, 97.
Brown' coal, 731.
Brucite, 114.
Brusblte, 377.
Bunsenlte, 76.
Bustamite, 674.
Byrichritc, 155.
Byssollte, 678.
Cncliolong, 137.
Cacoseno, 402,
Cainigorm, 135,
MINERALOGY
Chirlatite, ?4S.
ChUdnlte, 563.
ChloanUte, US.
Chlorite, 631.
Chi on told, 626.
Chlorocalcite, 63.
Chloropal, 667.
ChlorophsElte, 656.
Cblorophyllite, 585.
Chlorosplncl, 93.
Chodnefflte, 43.
Chondrarseuite,
395.
Cbondrodite, 462.
ChoQlcrite, 535.
Chrome ochre, 637.
Chromite, 69.
Chrysobeo'. 94.
ChrysocoUa, 491.
Chrysolite, 478.
Chrysopraie, 136.
Chrysotile, 649
CimoHte, 638.
Cinnabar. 193.
Cinnamon stOQ6,
Calai
, 404.
272.
Caledonlte, 850.
Calomel, 49.
Cancrinlte, 606.
Capovcionite, 612.
Ciubnncle, 493.
CamaUlte, 62.
Camat. 631.
Cjii-nclian, 135.
Cnrpholite, 65G.
Carphos(derite,333.
Cassiterite, 98-
CasslterotantaUte,
69 L
Castor, S73.
Cataplelte, 674.
Cat'a-eye, 135.
Ciiwk, 313,
Coladonlte. 660.
Celestlne, 315.
Centrolite, 488.
Cer-ugyrite, M.
Cerlno, 474.
Cerite, 484.
Cei'usslte, 286.
Currant ite. 130.
Chabastte, 608.
Clialcaiithtte, 333.
Chalcedony, 135.
Chalcolite, 439.
Chalcomenlte, 257.
Chalcophanite, 1?2.
Chalcophylllte, 4G5.
Chalcopyrite, 189.
Chalcoslderlto, 430.
Cbalcotrichlte, 73.
Chalk, 272.
Chnlyblte, 277.
CtiamolBito, 562.
Chert. 135.
Cblastolltc, 460.
Chlldrenfte, 432,
CliUonlte, 197.
Chlolite, 42.
493.
CipoUlno, 272.
Clarite, 246.
ClauBtballte, 161.
Clay ironstone, 277.
Glayfl. 629.
Clinochlore, 633.
Clfnoclase, 424:
Clintonlte, 624.
Coal3, 729-731.
Cobaltite, 143.
Cobaltspath, 279.
Cobalt yitilol, 327.
Coccinlte, 68.
Coccolite, 567.
Ccei-nJeolactin, 405.
Colopbonite, 493.
Coloradoite, 202.
Columbite, 693.
Condunite, 192.
Connellite, 72.
Copaline, 716.
Coplapite, 331.
Copper, 18.
Copperas, 324.
Copper-blende, 238.
Coqulmblto, 330.
Cordierite. 686.
Comwallite, 418.
Conindophyllitc,
533.
Coruodum, 81.
Cotton- stone, 623.
lite, 60.
Corelline, 188,
Crcdnerite, 102.
Crichtonite, 83.
Crocflllte, 622.
Crocolsite, 355.
Cronstedtite, 689.
Crook eoite, 167.
Cryolite, 40.
Cryopbyllfte. 617.
Cryptollte, 867
Cuban, 191.
Cube ore, 403.
Cuprite, 73.
Cuproplumblte,
159.
Cyanlte, 461.
Cymophane, 94.
Cj-prine, 47i
Danallte, 497.
Danburite, 495.
DarwinttP, 192.
Datholite. 467.
Davldsonite, 686.
Davlnc, .')06.
Dechentto. 378.
DclafoBslte, 73.
Delessite, 538.
Demidowlte, 492.
Ucrmattne, 555.
Desclolzlte, 414.
Dladochlte, 454.
Dialloge, 668.
Dialogue, 278.
Diamond, 13.
Diasporo, 107.
DIchroile, 685.
Dlckinsonltc, 892.
Dletrichite, 3ii.
Dibyrlte, 419.
Dimorphlte, 207.
Dlopslde, 567.,
Dioptase, 490.'
Dlphanlte, 622.
Dlpyre, 602.
Diacraalte, 178.
Distbene, 461.
Dolorolte, 273.
Domeykite, 192.
Dopplerlte, 728.
Dufrenlte, 399.
Dufrenoyiite, 223.
Duraogite, 451.
Dysanalyte, 683.
Dysluite, 91.
Eedemite, 458.
Edingtonite, 620.
Eblite, 421.
Eiaennlckelkles,
182.
Elteolite, 606.
Elaterite, 708.
Electnim, 25.
Eleonorite, 40L
lite, 113.
Embollte, 65.
Embrethite. 227.
Emerald, 81, 586.
Emerald- nick el
298.
Emery. 81.
Emmonite, 284.
Emplectite, 216.
Enargite, 245.
Enstatite, 563.
EosUe, 359.
Eosphorlte, 433,
Eplboulangerlte,
250.
Epichlorite, 533.
Epldote, 473.
Epigenlte, 249.
Epistilbite, 613.
Epaomite, 321.
Erinite. 418.
Eritbrosiderite, 65.
Eiythrite, 386.
Esmarkite, 585
Euchroito, 417.
Euclase, 46S.
Eucraslte, 643.
Eodialite, 673.
Endnophite, 606.
Eukairite, 168.
EukoUte, 673.
Eulyline, 498.
Euphylllte, 623.
Euscnite, 687.
Eransite, 406.
ETlgtoklte, 47.
Fahlerz, 237.
Fahlunite, 535.
Fairfleldite, 894.
Famatinite, 247.
Fargite, 623.
Faroellte, 626.
Faesalte, 667.
Faujasite, 607
Fayalite, 477.
Fellnite, 656.
FelBubanylte, 329.
Felspars. 680-697.
FCrberitc, 364.
FerguBonlte, 695.
Ferrotltanitc, 670.
Felbol, 655.
Flbroferrite, 331.
Flchtellte. 722.
FlUowltc, 390.
Fiorite, 137.
Flre-blendc, 252.
FIseherlte, 407,
Flint, 135,
FlueHltc, 39.
Flaocerine, 36.
Fluocerite, 35.
Fluorlte, Ouorispar,
33.
Forchhammei'lte,
C57,
Forccltc, 621.
Forsterite, 476.
Fowlerite, 674.
Fnnkllnltc, 6& I
Frenzelite,*210
Friedelite, 628.
Frleselte, 186.
Frieslebenlte, 22t.
Fuchtte, 619.
Fuller's earth, 632.
OadoHnite, 471.
Gahnlte. 91.
Galactite, 623.
Galena, 163.
Galmei, 485.
Garnet, 493..
Gaylussite. 392.
Gearksutite, 46.
Gehlenite, 504.
Gelbeisenerz, 346.
itc, 241.
Geradorflate, 147.
Glbbaite, 116.
Gleseckite, 585,
650,
Gigantolite, 585.
GUbertite, 619.
Giobcrtlte, 276,
Girasol, 187.
Gismondlne, 624.
Glagerite, 633.
Glaserite. 308.
Giauberite, 311.
Glaucodote, 144.
Glauconite, 659.
Glaucophi
Gmelinlte, 609.
Gold, 25.
Goslarite, 822.
Gbthite, 108.
Grammatite, 578.
Graphic granite,
562
589.
Graphite, 14.
Greenockite, 179.
Green 07 it e, 668.
Gmnauite, 154.
Grunerlte, 634.
Guanajuatlte, 201.
Guayaquillite, 718.
Guejarlte, 211.
Gummite, 120,
Gymnite, 647.
Gj-psum, 319.
GyroUte, 60J.
Hsematite, 62.
Hal dingc rite, 379.
Ralr-salt, 328.
Halite, 51.
Halloysite, 632.
Hamartite, 38.
Harmotome, 617.
Hartlne, 719.
Hartite, 723.
Hatchettlne, 721.
Hfitchettollte, 699.
Haaerite, 150.
Haugbtonite, G13.
Hausmannite, 99.
Hauyne, 610.
Haydenlte, 608.
Haytorite, 467.
Heliotrope, 135.
Helvlne. 496.
Hepatite, 813
Hereynlte, 92.
Herderitc, 452.
Hcrmannlte, 583.
Herrengrundlte,
848.
Herachellte, 611.
Hessite, 174.
Heterozlte. 391.
Hculandite, 614.
Hisingeritc, 659.
Ilislopite, 272.
Iljelmite, 696.
Ilomilite, 469.
Hopclte, 409.
Horbachltc, 156.
Ilomblcnd
Hymeaite. 383.
Homstone, 135,
569.
HUbnerlte, 366.
Iludsonite, 667.
Humboldt 11 Itc, 5
Hnmlte, 482.
HurcftulHe, 391,
Huronlte, 535.
57S.
Hyacinth,. 138.
Hyalite. 137.
Hyalophanc, 595.
Hyalosiderite, 478.
Hydrarglllite, 116.
Hydroboraclte, 270.
Hydroraagnesite,
293.
Hydrophane, 137.
Hydrophite, 652.
Hydrotaldtc, 118.
Hydrozlncite. 296
HygrophUite, 652.
Hypersthene, 6C5.
Hypochlorite, 667.
HypostUbite, 612.
Hypoxanthite, 661
Ice, 74.
Iceland Bpar, 272.
Ice-spar, 689.
Ichthyophthalmlte,
603.
Idocraae, 47S.
IdriaUte, 726.
Ilmenfte, 83.
IndicoUte, iCG.
Inverarite, 182.
lodlte, 57.
Jollte, 585.
Iridium, 28.
Irldosmluia, 82.
I rite, 89.
Iron, 16.
Iserine,64.
Ixolyte, 71?.
Jacobsite, 87.
Jade, 678.
JadeUe, 597.
Jalpalte. 171.
Jamesonlte, 222,
Jaroslte, 844.
Jasper, 135.
JeO'ersonite, 569.
Jet, 731.
Johannlte, 336.
Jordanltc, 236.
Joselte, 12.
Jullanite, 234.
Kaiuite, 352.
Kiimmererite, 632.
Kaolin, 629.
Karelinlte, 255.
Karstenlte, 312.
Keilhauite, 669.
Kermesite, 253.
Kicaerite. 320.
Kllbrickenite, 242.
Killinitc, 672, 651.
Kirwanito, 558.
Klaprothite, 220.
Kllpsteintte, 662.
KncbeUlte, 4S0.
Eobaltbescbtag,
366.
KobeUlte, 228.
KoUyritc, 634.
Komarit, 664,
Kong^bergite, 23.
Konlgine, 335.
KiinUte, 724.
Koppite, 631.
Kotschubeyite, M3.
Kottlgite, 387.
Krantzite, 713.
Kranrite, 399.
Krelttonltc, 91.
Kremerslte, 64.
Krlsuvigtte, 334.
KrokidoUte. 6S1.
Euhnlfe, 370.
Kupfcrblau, 492.
Kyroslte, 140.
Labradoiitc, 593.
L&narkite, 317.
Langlte, 835.
ithanlte, 303.
Lapls-lazull, 611.
Laalonifo, 405.
Latrobite, 591.
Laumontltc, 618.
Laurite, 204.
Lautitc, 172.
Lavcndulan, 386.
Lazulitr, 431.
Load'hUlite, S06.
Leadspar, 286.
Lebcrkles, 140.
Leellte, 689.
Lenzinltc. 632.
LeoobarUlte. 612.
Lepldolite. 618.
Lepldomelane, 514.
Lepolite. 691.
Lerbachite, 200.
Lettsomlte, iJ51.
Leuchtenbergite,
632.
Leuclte, 505.
Leucophane, 687.
Leucopyrite, 142.
Levyne, 610.
Lherzollte, 667,
Libethenlte, 411.
Liebenerlto, 649.
Liebigitc, 301.
Llcvrite, 483.
Lignite, 731.
Lime-mica, 622.
Limestone, 272.
Limnlte, 117.
Limonite, 110.
Linarite, 349.
Lindakerito, 299,
Linnjeitc, 152.
Liroconite, 43i
Lithiophlllte, 369.
Lithomarge, 631.
Llthofylon, 137.
Loam, 629.
Loweite, 338.
Luclissapphlr, 683.
Lacuilite. 272.
Lttdlamite, 389.
Lndwiglte. 265.
Lnmachello, 272.
Liinoburgite, 467.
Lunnite, 423.
Luzonite, 246.
Lydian stone, 135.
Magnesia-mica,
612.
Magncsio-ferrite,
86.
Magnesite, 275.
Magnetite, 85.
MagnoUtc, 354.
Malachite, 295.
Malacoiite, 567.
Malacone, 642.
Maldonite, 106.
MalJardite, 326.
Malthazlte, 633.
Manganese, red,
278.
Manganese -spar,
Mica, 512,
Microcline, 689.
Microlito, 684.
MlcroBommlte, 607.
Miemlte, 273.
Mllarite, 673.
MiUerite, 181.
Mlloacbln, 635.
Mlmeteslte, 446.
Minium. 104.
MirabUlte, 318.
Mlspickel, 141.
Misy, 33 L
Mlxite, 425.
Mizzonite, 50L
Molybdenite, 203
Molybditc, 127.
Molysite, 61.
Monazite, 368.
Monradite, 543.
Montanlte. 353.
Montebrasite, 450,
Monticellite, 481,
Montmoriilonite,
636.
Moonstone, 563,
Morcnositc, 323.
Morion, 135,
Morocochite, 213.
Morvenlts, 617.
Mosandrite, 672.
Moss-agate, 135.
Uottramite, 420.
Murchlsonite, 589,
Muriaclte, 312.
Muscovite, 519.
MuEsite, 567.
MyeUn, 681.
Nacrite, 630.
Nadorite. 762.
Nagyaglte, 195.
Naphtha, 707.
Natrolite, 622.-
Natron, 290.
Naumannite, 173.
Needle-ore, 231.
Nemalite, 114.
Ncpheline, 506.
Nephrite, 578.
Newberyite, 378.
Newjanskite, 31.
Nickel, at seulate of,
37L
Nickelerz, 372.
^'lckelite, 183.
Nltratlne. 268.
Nitre, 259.
Nltrocalcite, 26a
Nitromagnesite,
285.
Marble, 27J.
Uarcasite, 140.
Marcelinc, 100,
Margarite, 622.
Margarodlta, 619.
Mari, 272.
MarmoUte, 560.
Martite, 82.
Mascagnlne, 309.
Masonite, 527.
Massicot, 75,
Matlocklte. 66.
Maxite, 306.
Mcorachauni, 644,
Megabasite, 360.
Melonltc, 600.
Mclaconlte, 79.
MclanitO, 493.
Melantcritc, 33«.
Meltnophanc, 668.
Molllllte, 503.
MeUite, 704.
Melonlto, 193.
Melopsite, 631.
Mcndlpltc, 67,
Moncgblnltc, 335-
Mcngltc, 690.
MenUlte, 137.
Mercury, 20.
Mcaolltc, 623,
Meteoric iron, 16.
Mlargyrlte, 212.
261.
Nohllte. 698.
Nontronite, 657.
Kosean, 509.
Ocbran, 665.
<Erstedlt«, 675.
Okenlte, 602.
Ollgoclase, 592.
OllTenile, 412,
OliTiDC, 478.
Oncosin, 648.
Oolite, 272.
Ooslte, 585.
Opal, 136. 137.
Orangite, €45.
Orpimcnt, 206.
Orthite, 474.
Orthoclase, 539.
Osmirldium,81.
Oltrclite, 528.
OxaJitc. TOO.
Oihavecrite, C03.
Ozocerite, 720.
Pachnollte, 44.
Paisbergite. 574.
ralladium, 29.
Paraffin, 720.
Puragonlte, 520.
Pargasite, 576.
Parlsito, 305.
Paulitc, 665.
Pcctolite, 698.
Pcganite, 408.
Pel lorn, 685,
Pennine, 532.
Pcntlandite, 181
PercyUte, 71.
Periclase, 75,
Pcricline, 69a
Peridote. 47a 1
PerovBklte, 6801
Petal Ite, 573.
Petroleum, 707.
Petuntze, 589.'
Pctilte, 176.
PhacoUte, 608.
Pharmacolite, 361.
Pharmacoalderite;
403.
Phenacite, 469.
PhiUipsit*, 616.
Phlogoplte, 616.
Phoonico-chrOitei
356.
Phosgenite, 804.
Phosph orochalclte,
423.
Piauzlte, 711.
Pickering! te, 34 L
Picotlte, 93.
Picrolite, 649.
Picrophyll, 541.
Picrosmlne, £42.
Plcdmontite, 473.
PUoHte, 580.
Pimelite, 548.
Pinguite, C58.
Pinite, 685.
Pinltoid, 654.
PlsoUte, 2''2.
Pissophanc, 332.
Pitch blende, 90.
Pitticite, 455.
Plagiooite, 219,
Plasma, 1S5.
Platinlridinui, 27.
Platinum, 26.
PlattnTrite, 103L
Pleonaste, 93.
Plinth! tc, 655.
Plombgomrae, 442.
Plumbocalcite, 27i
PlumboEtib, £27.
Pollux, 606.
Polyargj-ritc, 244
Polybasitc, 243.
Polycrase, 686,
Polydymlte, 154
Polyhalile,-840.
Polyhydrite, 659.
Polyipignite. 689L
Polytelite, 239.
Porcelain earth,
629.
Prase, 135.
Praseolite, 685.
Prchnite, 627,
Prosoplte, 48.
ProuaUte, 226:
Psilomelane, 121»
PBlllaclnite, 374.
Pucheritc, 375.
Puffierife, 619.
Pycnlte, 463.
Pycnotrop, 536L
Pyrallolite, 554.
PyrargillUc, 5S5.
Pyrargyrlte, 225.
P.\ rite, 139, 140,
151, 186, 189.
Pyroaurite, 119,
Pyrochlore, 684.
P)Tochrolto, lis.
Pyrolusitc, 101.
Pyromorphltc-444.
I'yrope, 493.
PyrophylUte, 640.
Pyrophysalite, 463.
Pyropissite, 720.
Pyrorclinlto, 714.
Pyrorthltc, 474.
Pyroscleritc, 534.
PyrosmalKc, 629.
PyroBtilpnlte, 252.
Pyrc'xcno, 657.
Pyrrhile, 684,
Pyrrhotlto, 15L
Quartz, 135.
RammcUberglte,
149.
lUzoom oITskln, 637
M I N— M I N
431
Realgar, 20£.
Reildlngite, 396.
IMlle, 83.
RMlnulUtc, 1C4.
Reinite, 3S3.
Rclnlts, (13.
R«ins, 707-138.
Reunite, 714.
Rensalne, 337.
RlutlUe, as.
Rhodlzlle, 364.
Rhodochrome, 633.
Rhodonite, S74.
Rlpldolitc, 633.
RLIUiigerite. 187.
RiTotite, 703.
Rock-crystal, 135.
Bock-salt, 61.
Rock soap, 655.
Romaozowite, 483.
Romelte, 700.
RoscocUtc 678.
Rosellte, 380.
Rothofflte, 493.
Riittlslle, 6S4.
Rubellan, 613:
KubeUIte, 46&
RuUcella, 93.
Kuby, 81, 93.
RntUe, 95.
Sahllte, 6«7.
Salmlac, 62.
Salt, SL
Saltpetre, 259.
Samarskite, 697.
Sandliergente, 631.
!saIlilUn^ 589.
Saponlte, 548.
Sapphire, 81.
Sapphire d'eau,
685.
Sapphlrtne, 93.
Sapphidte, 465.
SarcoUtc, 490.
SartoHte, 214.
SassoUne, 105.
Satin-spar, 28L
Satissurite, 597.
Savon da verrler,
lOL
Saynite, 154.
ScapoUte, 502.
Scarbroite, 634.
Scheelite, 361.
Scheererite, 735.
Schiller spar, 564.
ScMrmerite, 330.
Schneebergite, 700.
Schnelderlte, 33:
Schorl, 466.
Schorlomite, 670.
Schwartzember-
gite, 68.
Scoledto, 633.
Scorodite, 397
Selenite, 319.
Selenium, 3.
Selensulphnr, 3.
Senarmontlte, 134.
Serpentine, 549,
Shale, 629.
Siderite, 135, 277.
SldenMchlsolite,
539.
Siderostlidte, 661.
Siesenite, 16i.
SiUimanlte, 462:
SUvcr, 31.
Sinter, 137.
Slsserskite, 33.
Skntte'rndite, 157.
SUtc cUy, 629.
Slate spar, 373.
Smaltine; 145.
Smlklte, 325.
Smlthsonite, 380.
Soda-chabasite,
609.
Sodalite, 608.
Soda-mica, 530.
Spadaite, 646.
Spar, heary. 313.
Spathiopyrlt'
165.
143.
Sphe
Spinel, 93.
Spodomene, 571
Stanolte, 185.
Stasstm-tite, 263.
Staorolite, 464.
Steatite, 540.
Steinhellite, 585.
'tephanlte, 240.
Stemberglte, 186.
Slibiconite, ISO'
Stibnite, 203.
Stilbile, 618.
Stilpnomelane, 661.
jStolpenlte, 655.
Stolzile, 362.
Strahlstein, 578.
Strengite, 398.
Stromeyeritc,
Strontianitt 384.
StniYite, 423.
Studerite, 333.
Stylotyp, 332.
Succinite, 713.
Sulphur, 1.
Sunstone, 593.
Surturbrand, 731.
Susannlte, 307.
Sussexite, 271.
Svanbergite, 463.
SyWanlte, 194.
SylTltB, 60.
Sympleaite, 385.
Syngenlte, 339.
Szaboite, 576.
Szaibelylte, 269.
Tabergite, 632.
Tabular spar, 666.
Tachhydrite, 63.
Tagilile, 416.
Talc, 540.
Talcosite, 640.
TalUngile, 70.
Tantalic ochre, 134.
Tantalite, 691.
Tapiohte, 692.
Telluric bismuth, 9.
Telluric Iron, 16.
TeUnrlte, 133.
Tellurium, 4; blacli.
I 195; graphic,194.
Tennantlte, 238L
Tenorite, 80.
Tephroite, 479,
Tetradymite, 10.
Tctrahedrite, 237.
Tharandite, 273.
Thenardite, 310.
Thermonatrlte, 289.
Thomsenolite, 45.
Thorasonlte, 626.
Thorite, 644.
Thraulite, 659.
Thrombolite, 703.
Thulite, 472.
Thuringtte. 537.
Tiemannlte, 199.
Tilkerodite, 161.
Tin, 15; ores of,
98.
Tinder-ore, 129.
Tinkal, 266.
Titaoomorpbite,
679.
Tobennorite, 601.
Tocomadite, 59.
Topaz, 81. 463.
Torbanite, 737.
Tourmaline, 466.
Travertlno. 272.
TremoUte, 578.
Tnclaslte, 585.
Tridymite, 136.
Triphylite, 369.
Triplite, 448.
Trlploidite, 393.
Tripnkeite, 469.
[Trltomite, 646.
TrOgertte, 437.
Trona. 291.
Troostile, 487.
Tschewkinile, 671.
Tufa, 272.
TnngsUte. 128.
Turgite. 106.
Tumerite, 308.
Turquoise, 404
Tyrile, 695.
Tyrolite, 423.
Ulexlte, 368.
UUmannlle, 148.
Umber, 661.
Uranlnile, 90.
Uranite, 436.
Uranociicite, 433.
Uranophane, 6G5.
Uranospinite, 437.
Uraootantalite, 697.
Cranothorite, 644.
Cranotile, 666.
Uran-Titriol, 336.
Urao, 291.
tJrusitc, 346.
Uwarowlte, 493.
Valentinelte, 125.
'anadine-bronzite,
568.
Vanadinfte, 445.
Variscite, 406.
Varriclte, 101.
Vauquelinite, 357.
Venus' hair, 95.
VeazelyUe, 413.
VilUnUa,SM.
Vitriol, green, 324 ;
red, 347; white,
333.
Vitriol ochre, 33L
Virlaolt^ 384.
Voglite. 300.
Volborthlte, 416.
Volgerite, 131.
Volulte, 342.
Voltxine, 254.
Vulplnite, 312.
Wad, 121.
Wagnerite, 447.
Walchowite, 715.
Walkerite, 599.
Walpurgite, 441.
Wapplerlte, 382.
Warringtonite, 335.
Washingtonltc, 83.
Water. 74.
Wavellite, 405.
Websterite, 339.
Wehrlite, 11.
Weissgiltigerz, 339.
Weisaite, 685.
Whewelllte, 706.
Whitneyite, 193.
Willemlte, 486.
Wiserlne, 366.
Withamite, 473.
Witherite, 382.
Wittlchenile, 239.
Wohlerite, 678.
Wiilcblte, 230.
WoUnmUe, 364.
WoUiberglte, 217.
Wolkontkoitc, 663.
Wollastonitc, 566.
Woodwardite, 351. .
Wnlfanite, 358.
Wurtzite, 178.
Xanthocon, 251.
Xanthoiite, 464.
Xanthophyilite,
525.
Xanthosiderltc,
IIL
Xenotlme, 366.
XunotlUe, 600.
Xylite, 660.
Yellow earth, 665.
Tttroccrite, 34.
enite, 697.-
Tttrotantalite, 694.
I'ttrotitanite, 669.
Yn. C27.
ZaraUte, 396.
Zeagonite, 625.
ZeoUtes, 598-626.
Zepharovicbite, 406. .
Zeunerite, 440.
Zinc, 17.
Zlndte, 77.
Zinckenlte, 215.
I Zinnxraldite, 517
I Zircon, 138.
1 Zoisite, 472.
Zorgite, 162.
' Zundererz, 132;
I Ziriesellte, 449.
I (3t F. H.)
MINERAL WATERS. No absolute line of demarca-
tion can be drawn between ordinary and mineral waters.
There is usually in the latter an excess of mineral con-
stituents or of temperature, but some drinking waters
contain more mineral constituents than others that
are called mineral waters, and many very pure waters,
both cold and warm, have been regarded for ages as
mineral springs.
As to the origin of mineral waters, there is much in
what the elder Pliny said, that waters are such as the soil
through which they flow. Thus in limestone and chalk
districts an excess of lime is usually present; and the
waters of a particular district have much resemblance to
each other — as in the Eifel, in Auvergne, and in the
Pyrenees. But this is only a partial explanation, for
waters are by no means necessarily uniform throughout a
particular geological formation. We do not know with
any certainty the depth from which various mineral waters
proceed, nor the various distances from the surface at
which they take up their different mineral constituents.
The source of the temperature of thermal waters remains
a subject of much uncertainty. Among the assigned causes
are the internal heat of the globe, or the development of
heat by chemical or electrical agencies in the strata through
which they arise.
Their occasional intermittence is doubtless often depend-
ent on the periodical generation of steam, as in the case
of the Geysers. A few geological facts are certain, which
bear on the origin of mineral waters. Such springs are
most abundant in volcanic districts, where many salts of
soda and much carbonic acid are present. They occur most
frequently at meetings of stratified with unstratified rocks,
in saddles, and at points where there has been dislocation
of strata.
The diffusion of mineral waters is very extended. Pliny
was quite correct in observing that they are to be found
on alpine hrights and arising from the bottom of the
ocean. They are found at the snow in the Himalayas and
they rise from the sea at Baiae and Ischia. They are to be'
found in all quarters of the globe, but more particularly
in volcanic regions, as in the Eifel and Auvergne, in the
Bay of Naples, and parts of Greece, in Iceland, New
Zealand, and Japan. But there are few countries in which-
they are not to be found, except in very flat ones and in
deltas of rivers, — for instance, in the north of France, where
they are very few, and in Holland, from which they are ab-
sent. France, Germany, Italy, and Spain, as well as Greece,
Asia ilinor, and the Caucasus, are all rich in mineral waters..
The British Isles have a fair though not very large pro-
portion of them. There are a few in Sweden and Norway.
They are abundant in the United States, less so in Canada.
They are found in the Azores and in the West India.
Islands. Of their occurrence in the interior of Africa or
of Australia we know little ; and the same is true of South
America. But they are met with in Algiers, in Egypt, and
in the Holy Land. The vast Indian peninsula has for its
size a comparatively ^lall supply.
As the effects of mineral waters on the bodily system,
have been found to be different from those of drinking
waters, an explanation of this has been naturally sought
for. It has been imagined that there is something special,
in the nature of mineral waters, that their heat is not
ordinary heat, that their condition is a peculiar electric
one. Some French modern writers even say that they have
a certain life in them, that their constitution is analogous
to that of the serum of the blood. But we must pass by
these speculations, and be guided as far as possible by ascer-
tained facts, respecting the action on the system of water,
of heat and cold, and of the mineral constituents present.
Mineral waters, when analysed, are found to contain a
great many substances, although some of them occur only
in very minute quantities : — soda, magnesia, calcium,
potash, alumina, iron, boron, iodine, bromine, arsenic,
lithium, caesium, rubidium, fluorine, barium, copper, zinc,
manganese, strontium, silica, phosphorus, besides extractive
matters, and various organic deposits known under the
name of glairin or baregin. Of gases, there have been
found carbonic acid, hydrosulphuric acid, nitrogen, hydro-
gen, oxygen, and ammonia. Of all these by far the most
important 4n a therapeutic point of view are sodium,
magnesia, and iron, carbonic acid, sulphur, and perhaps
hydrosulphuric acid. These substances, detected separately
by chemists, are in their analyses combined by them into
various salts, if not with absolute certainty, undoubtedly
432
wi'.h a close approximation to it. Those combinations are
vc;y numerous, and some waters contain ten to twenty of
til' in; but there are always some predominating ones,
wl'ich mark their character, while many of them, such as
c: jium, rubidium, or fluorine, occur in mere traces, and
c;i!i not be assumed to be of any real importance. Mineral
waters therefore resolve themselves into weaker or stronger
solutions of salts and gases in water of higher or lower
temperature. For medical purposes they are used either
externally or internally, for bathing or for drinking. As
the quantity of salts present commonly bears but a very
small proportion to that of the fluid containing them,
water becomes a very influential agent in mineral-water
treatment, about which it is therefore necessary to say
something.
Tor the action of hot and cold baths the reader is referred
to ihe article Baths. But it may be observed here that,
according to the most generally received opinion, the cuta-
nooiis surface does not absorb any portion of the salts in a
mineral-water bath, although it may absorb a little gas
(an alkaline water, for instance, at most acting as a slight
dftergent on the skin), and that neither salts nor gases
have any action on the system, except as stimulants of the
E!cin, with partial action on the respiratory organs.
It seems to be ascertained that drinking considerable
amounts of cold water reduces the temperatiu'e of the body,
diminishes the frequency of the pulse, and increases the
blood pressure temporarily. Water when introduced
inlo the stomach, especially if it be empty, is quickly
absorbed ; but, although much of the water passes into the
veins, there is no proof that it ever produces in them, as is
Bomclimes supposed, a state of fluidity or wateriness.
Therapeutically, the imbibition of large quantities of water
leads to a sort of general washing out of the organs. This
produces a temporary increase of certain excretions,
augmented diuresis, and a quantitative increase of urea,
of chloride of sodimn, and of phosphoric and sulphuric
acids in the urine. Both the sensible and the insensible
perspirations are augmented. A draught of cold water
undoubtedly stimulates the peristaltic action of the
intestines. On the whole water slightly warm is best
borne by the stomach, and is more easily absorbed by it
than cold vrater ; and warm waters are more useful than
cold ones v/hen there is much gastric irritability.
In addition to the therapeutic action of mineral waters,
there are certain very important subsidiary considerations
which must not bo overlooked. An individual who goes
from home to drink them finds himself in a different
climate, with possibly a considerable change in altitude.
His diet is necessarily altered, and his usual home drinks are
given up. There is change in the hours of going to bed and
of rising. He is relieved from the routine of usual duties,
and thrown into new and probably cheerful society. Ho
takes more exercise than when at home, and is more in the
open air, and this probably at the best season of the year.
So important has this matter of season and climate been
found that it is an established axiom that waters can be
used to the greatest advantage during the summer months
and in fine weather, and during the periods most convenient
for relaxation from bu.siness. Summer is therefore the bath
season, but of late years provision has been made in many
places, with the aid of specially constructed rooms and
passages, for carrying out cures satisfactorily during the
winter season, e.</., at Aix-la-Chapelle, Wiesbaden, Baden
Baden, Baden in Switzerland, Dax, Vichy, and Bath. The
ordinary bath season extends from the 15th of May to the
20th or 30th September. The season for baths situated
at considerable elevations commences a month later and
terminates some ten days earlier. Mineral waters may be
Sjnployed at home, but patients seldom bo use them ; and
MINE E A L VV'; A T E E S
this necessarily limits the time of their useT' It is commoa
to declare that the treatment should last for such or such
a period. But the length of time for which any remedy is
to be used must depend on its effect, and on the nature of
the particular case. It is found, however, that the con-
tinued use of mineral waters leads to certain disturbances
of the system, which have been called crises, such as sleep-
lessness, colics, and diarrhcea, and to skin eruptions known
as la poussee. ' This cause, and also certain peculiarities of
the female constitution, have led to the period of three
weeks to a month being considered the usual period for
treatment. A certain after-treatment is often prescribed
— such as persistence in a particular diet, visiting springs
or climates of a different and usually of a tonic character,
or continuing for a certain time to drink the waters at
home. It may be added that the advantage of having
recourse to mineral waters is often felt more after than
during treatment.
Since improved methods of bottling have been discovered,
and the advantage of an additional supply of carbonic acid
has been appreciated, the export of waters from their sources
has increased enormously, and most of the principal waters
can now be advantageously used at home. It may be
added that many of the artificial imitations of them are
excellent.
The history of the use of mineral waters can only jusl
be alluded to. They have been employed from the earliest
periods, and traces of Koman work, have been found al
most of the European baths which are now in favour, — at
almost all the thermal ones. Occasionally new springs
are discovered in old coimtries, but the great majority ol
them have been .long known. They have varied in
popularity, and the modes of applying them have alsd
varied, but less so than has been the case with most of the
ordinary medicines. Warm waters, and those containing
small quantities of mineral constituents, appear to have
remained more steadily in favour than any other clasi
within the appropriate sphere of mineral waters, which L'
limited to the treatment of chronic disease.
The attempt has been made to range mineral watcn
according to their therapeutic action, according to theii
internal or external use, but most generally according t(
their chemical constituents so far as they have been fron
time to time imderstood; and a judicious classificatioi
undoubtedly is a help towards their rational employment
But their constituents are so varied, and the gradationi
between different waters are so finely shaded off, that i
has been found impossible to propose any one . definiti
scientific classification that is not open to numberles
objections. Thus a great many of the sulphur waters ar
practically earthy or saline ones. Yet because they con
tain very minute amounts cf such a gas as hydrosulphuri
acid, an ingredient so palpable as always to' attrac
attention, it is considered necessary to class them unde
the head of sulphur. The general rule is to attempt t
class a water imder the head of its predominant element
but if the amount of that be extremely small, this leads t
such waters as those of Mont Dore being classified a
alkaline or arseniated, because they contain a very littl
soda and arsenic. The classification in the following table
which is that usually adopted in Germany, has the meri
of comparative simplicity, and of freedom from theoretica
considerations which in this matter influence the Frenc;
much more than the German writers. The more imi)ortau
constituents only are given. The amount of solid constitv
ents is the number of parts to one thou.sand parts of th
water ; the tomi>eratiiro of thermal s])ring3 is added. Th
waters are cla.ssified as indifferent, earthy, salt, sulphurettec
iron, alkaline, alkaline saline — with subvarieties of tabl
waters and purging waters.
MINERAL WATERS
Table 1.— Typical Mineral Waters.
433
Solids.
Bicarbonate of soda.
,, potash...
t, magnesia.
,, calcium...
Sulphate of soda
,, potash
,, magnesia
,, calcium
Sulphide of sodium
Chloride of sodium
,, potash
,, magnesia
Carbonate of iron
Silicic acid
Gases,
Carbonic acid
Hydvosulphmic acid
•0017
•0195
•0208
•0135
•0005
■0496
•013
•012
•050
•038
Sail.
Eiasingen.
•389
552
:Satl.
Sea-Water.
2^38
296
•25
25 21
3-39
Sulphui
Alx-la-Chapelle,
•6449
•0506
•0136
2-616
Scbwalbach.
•0206
■2122
■2213
•0079
•0037
•0837
•0320
Alkaline.
Vichy,
4 883
•352
•303
•434
•292
Alkaltnt.
Saline.
CarUhad,
•16
1^03
•003
159
16^0
In addition to their solid constituents, gas is present in
many waters in considerable qnantity. There is a little
oxygen and a good deal of nitrogen in some of them. ; the
quantity of hydrosulphuric acid, even in strong sulphuric
waters, is wonderfully small ; but the volume of carbonic
acid present is oft^n very large, — for instance, in the case of
Kissingen, Schwalbach, and Selters. Carbonic acid is so
generaUy diffused that it is practically a very important
agent in the therapeutics of mineral waters. Springs that
contain it are far the most agreeable to the taste, and
consequently most popular with patients. The immediate
effect of the carbonic acid which they contain is that of
pleasant stimulation to the stomach and system, although
it can scarcely be said to approach, as some have thought,
the slighter forms of stimulation from alcoholic drinks.
Extremely little appears to be known of its actual operation
on the systom : a part of what is swallowed is returned by
eructation, and a part passes on to the intestines ; whether
any appreciable quantity reaches the blood is doubtful.
There is no question that carbonic acid increases diuresis.
Practically it is found to aid digestion, helping the functions
of the stomach, and in a slight degree the peristaltic action
of the intestines. The increased flow of urine may be
caused by its favouring the absorption of water by the
stomach. In some baths carbonic acid is so abundant that
precautions have to be taken to prevent its tendency to
iccumulate on account of its heavy specific gravity. Car-
bonic acid gas, used as a bath, proves stimulating to the
skin and to the general system ; but its employment has
not answered the expectations formed of it.
Indifercixi Waters scarcely vary iji chemical qualities from ordi-
nai-y drinking water ; but they are usually of higher temlioraturo.
Their therapeutic action, which is mainly exercised through baths,
has been explained on the theory of peculiarities of their electric or
thermal condition, about which we know nothing definite, and on
tlie presence in some of them of a large quantity of nitrogen. It
has also been ascribed to the various organic substances in some of
them, such as glairiu, which when collected is sometimes useful as
a cataplasm. These waters are not often much drunk, but any
efficiency they may have in dyspepsia and perhaps in neuralgic
diarrhoeas must be attributed to tlie favourable action of hot water
on the digestion. The waters of this class, especially the hotter
ones iu the form of baths, are extremely useful in resolving the
effects of inflammation, in thickenings of the joints, <ind in chronic
rheumatism and gout. Tliey also are often eH'ectivc, especially the
cooler ones, in neuralgia and in some hysterical affections. Tliey
are somet'mcs prescribed in urinary aftcctions, in which case they
probably assist o^- dilution. The effects of many of these waters are
, aided by the baths often being situated at considerable elevations
and in out-of-the-way spots, whence the Germans' called them
Wildbader. They are very widely diffused, being found iji all
quarters of the globe, especially in volcanic districts. There arc
many in New Zealand ; iu America the hottest are iu the West and
in California.
1&— ir
Table U.'^—Indiferent W.ilers.
Evian, Lake of Gene?
Badenweiler, Baden .
Buxton, England
Sclilangenbad, Na^sai
Sacedon, Spain ,
Wililbad, Wlirtcmberg.
PfelTeifl, Switzerland...
Ragatz, do.
Panticosa, S. Pyrenees.
Teplitz, Bohemia
Gastcin, Austria
101-120
35-118
For what prescribed.
I Nei-vous cases, dyspepsia, urinary
[ affections.
I For mild rheumatic treatment : a
[ health resort.
Gout and rbeumatism fnitrocen
, present).
Nervous cases, female disordei-s. skin.
Rheumatism, gout, cutaneous aflec-
Gout and rheumatism, neuralgia,
thickenings.
Do. (nitrogen present); special action
in phthisis.
Gout, rheumatism, old injuries, jolnia
Do. do.; soothes nervous system.
Earthy Waters.— These differ chiefly from the indifferent waters
m containing an appreciable quantity of salts, among which sulphate
or carbonate of lime or of magnesia predominates. The great
majority of them are of high temperature. They produce the same
effects as the indifferent waters, but are perhaps less efficacious
in neuralgic affections, while they are more employed in some of
the chronic scaly eruptions. There was formerly a tendency to
c«nsider these waters useful in urinary affections ; but at the
present day it is only the colder ones that have come into repute
for tlie expulsion of gravel and biliary calculi and in the treat-
ment of affections of the bladder generally. Some of them have
also of late years been considered to exercise a favourable influence
on scrofula, and to be useful in the early stages of pulmonary
phthisis. This has been attributed to the salts of lime present in
them, although it is known that most of its salts pass throuo-h the
system unaltered, llany of tliese baths, sncli as Leuk and Bormio,
enjoy the advantages of great elevation, but Bath, othenvise one of
the best of them, lies low.
Table IU.— Earthy Waters.
Locality.
Contrexerille, Vosgcs
Lippe Springe, N. Germany
Wildungen, do.
Wclssenbcrg, Switzerland...
Pougues, France
Baden, Switzerland 1,1S0
Leuk. do 4,400
Bormio. Xorth Italy 4,400
Lucca, Italy '
Batli, England 1 ...
Dus. toiitli of France 1,400
B. do Bigoires, Pyrenees l.SOO
Temp.
03-123
66-104
lOS-122
lOS-122
I calculous
\ affections.
( Supposed to be useful in
^ phthisis.
Special use in urinary com*
, plaints; contains iron,
f Resorted to for pulmonary
( affections.
Dyspepsia, diabetes, hepatic
and urinary concretions,
f Rheumatism, gout, paraly.
^ is. scaly crupiions.
some female comiilainfs.
do. ; old sprains. 1
G4-123 I Do.; chlorosis. neuralgia.
' In this and the following tables a selection is given of some of the best-known
mineral waters in various European coaiitrics that possess establislimcnts. Their
chief pcculiurities of elevation, of temperature, and constituenis are briefly noted
The curative effects, necessarily alluded to very generallv. are those usually
ottribnted to them.. ^"ou.
434
M I N E R"A L W A T E R S
Salt, ffaiers are so called from containine a predominant amount
of chloride of sodium. T"'-iy also generally contain chlorides of
magnesia and of limo, and occasionally small amounta of lithium,
bromine, and iodine. They further often contain a little iron, which
is au important addition. The great majority of the drinlcing wells
have a large supply of carbonic acid. There are cold and hot salt
springs. Sometimes they are used for drinking, sometimes for
bathing ; -and the double use of them is often resorted to.
The normal^ quantity of*conimon salt consumed daily by man is
usually set down at about 300 grains. The maximum quantity
likely to be taken at any well maybe 225 grains, but commonly not
more than half of that amount is taken. The increase to the usual
daily amount is therefore probably not much more than one-third.
Still it may be presumed that the action of a solution of salt on an
empty stomach is different from that of the same amount of salt
taken with food. Salt introduced into the stomach excites the
secretion of gastric juice, and favours the peristaltic actions, and
when takeu in considerable quantity is distinctly aperient. We
thus see how it is useful in dyspepsia, in atony of tho stomach and
intestines, and sometimes in chronic intestinal catarrh. Salt when
absorbed by the stomach appears a^in in the urine, of which it in-
creases the amount both of fluid and of solid constituents, especially
of the urea. It seems therefore to be pretty certain that considerable
quantities of salt taken into the circulation increase the excretion
of nitrogenous products through the urine, and on the whole
accelerate the transformation of tissue. Salt is thus useful in
Scrofula by stimulating the system, and also in anaemia, especially
when iron is also pi-esent. In some German stations, as at Soden,
carbonated salt waters are considered to be useful in chronic
laryngitis or granular pharyngitis.
• Baths of salt water, as usually given, rarely contain more than 3
per cent, of chloride of sodium, some of the strongest perhaps from
8 to 10 per cent. Their primary action is as a stimulant to the
skin, in which action it is probable that the other chlorides,
especially that of calcium, and still more the carbonic acid often
present, co-operate. In this way, and when aided by various pro-
cesses of what may bo termed water poultices and packing, they
are often useful in removing exudations, in chronic metvitis and
in some tumours of the uterus, and generally in scrofula and rachitis,
and occasionally iu some chronic skin affections.
Tho French accord Ivigh praise to some of their thermal salt
waters in paralysis, and some German ones are used in a similar
way in spinal affections. The salt waters are sometimes so strong
that they must be diluted for bathing. In other cases concen-
trated solutions of salt are added to make them sufficiently strong.
These waters are v»ridely diffused, but on the Vi-hole Germany is
richest in them, especially in such as are highly charged with
salt. The Kissingen springs m.ay be considered as tj'pical of ihe
drinking wells, and sea-water of bathing waters. The air of salt-
works and pulverization of the water are employed in German
baths as remedial agents.
Salt springs are found in many quarters of the world, but the
chief can)onated groups for drinlcing purposes occur in Germany,
and at Saratoga in America, where very remarkable wells indeed
are to be found. France and England have no springs of this
class. The stronger wells, used chiefly for bathing, occur where
Table 1Y. —Salt ,S;;rni.7s.
i
Locality.
Hombiug, do
KlssinReii, Bavaria
Pynnont, Noitii Germany..
114-149
116-6
Kreuznach, near Bingcn.
"Wiesbaden, Noss-iu
Baden-Baden
Bourbonne, Haute-Marni
Balanic, South France...
Sallns, Moutlcrs. Savoy (USO ft.)
Biidca, Savoy (1700 ft.) 95
Acoul, Korth Italy 169
Abano, do 18S
Coldna da Mombuy, near 1 1 155.158
Barcelona ) .
Costona, Guipuzcoo, Spain 83-94
Therapeutic Action.
Dyspepsia, aniemla, sci'ofula,
special for tliroat and phthisis.
Dyspepsia, slighter hepatic
affections, chlorosis, goul.
In all essentials the same.
Better known for its Iron; has
a good salt drinking spring.
Aealt wellwlth'mt carbonic acid
used in acrofula and nnxraia;
bathing more Important.
Used In dyspepsia ond gout; the
bathing is most Important.
Stillmllderwater; uses similar ;
gout.
nheumatUm, neuralgia, eEFects
of malaria.
Do. ; special for treatment of
paralysis.
Scrofula, untemla, loss of power,
sexual disordcra.
Act on liver and digestive Canal ;
used for obesity.
Rlicumntism; special treatment
with tho bull! deposit.
Chiefly 09 balhs; mud of bath
uied for poultice,
nheumntlsm, stlatica, old in-
juries.
Uluumatlsm, Indigestion, bron-
chitis.
Almost all the abovo fltaliona have several sprlnc^ of vailourt strengilis : tho cold
may bo said to vary from H to 5 8 per cent, of clilorldo of 6odlum ; Iho warm aie
generally 'leaker, perhaps varj-lng from 6-8 to l"6.
there are salt-bearing strata, as in Germany, Galicia, Italy, Switzer-'
land, France, and England. Very powerful waters of this class are
those of St Catherines in Canada.
The presence of minute portions of iodine or bromine in salt
waters is by no means infrequent, and they appear in considerable
quantity in some few. It is, however, e.^tremely doubtful whether
any known spring contains a sufficient quantity of iodine, still more
of bromine, to act specially on the system, even if that action were
not necessarily superseded by the presence of the large quantity of
other salts with which they are associated. Some of the best known
springs of the kind are : — Challes, "Wildcg^, Castrocaro, Hall, Adel-
htid's Quelle, Krankenheil, Kreuznach, Woodhall Spa. ■ .-. ■ 4
IrOn or Chalybeate iVatcrs. — Iron usually exists in waters in the
state of protoxide or its carbonate, less frequently as sulphate or
crenate, and very rarely if at all as chloride. The quantity jiresent
is usually extremely small. It may be said to vary from '12 to "03
in tho 1000 parts of water. Some wells considered distinct chaly-
baates contain less than '03. ilany wells, especially in Germany,*"
have a rich supply of carbonic acid, which is unfortunately wanting
in French and Knglish ones. - ' '■
It has long been the prevalent idea that want of iron in the blood
is the main cause of chlorosis and of other anremic conditions, and
that these conditions are best relieved by a supply of that metaL
Since the (detection of it in htenioglobuline tliis view has been still
more popular. It is pretty certain that the blood contains 37 to
47 grains and the whole system 70 to 74 grains of iron ; and it
has been calculated that in normal conditions of the system some-
what more than one grain of iron is taken daily in articles of food,
and that the same amount is passed in the faces; for although the
stomach takes tlie iron up it is excreted by the alimentary canal
mainly, it being doubtful whether any is excreted in the urine. It
is possible by drinking several glasses to take in more than a grain
of carbonate of iron in the day, equivalent to half that amount of
metallic iion. It has further been ingeniously reckonedfrom practice
that 10 to 15 grains of metallic iron suffice to supply the deficiency
in the system in a case of chlorosis. It is thought probable that
a portion of the iron taken up in water is in certain pathological
states not excreted, but retained in the system, and goes towards
making up the want of that metal. But, \vhether this or any other
explanation be satisfactory, there is no question as to the excellent
eflects often produced by drinking chalybeate waters (especially
when they are carbonated), and by bathing in those which are rich in
carbonic acid after they have been artificially heated. As regards
the drinking cure we must not, bowever, forget that carbonate and
chloride of sodium, and also the sulphate, are often present and must
be ascribed a share iu the cure. Thus chloride of sodium is a power-J
T.\BLE Y.— Stronger Salt }Vatcrs.
Chloride of
Sodium m
1000 parts
of Water.
Thcpapeutic Appllcatloo. - '
Rhcinfeld, Aargau, Switzerland
311
256
256
235
224
156
36
235-6
, 30-4
24-85
29
f Scrofula, effe.tsof Inrtairma-
tion. chronic cxudoliens.
some chronic cxantlic-
maa, rheuraotlsm, uterine
\ Infiltrations.
Do. da
Do. do.
Do. do.
Do. do.
Do. de.
Do. do
Do. do.
(Do.; special use in locomo-
\ tor aUxla.
Do. do.
Reiehenhall, near Salzburg (ISOO ft.)
Castrocaro, Tuscany
Droitwich, ne<ir 'Worcester
Xfluhelm. AVetterau (80'-i03' F.) ....
TAr
LEVI.
—Iron
Waters.
Locality
Height
in Feet.
Carb.
o( Iitjn.
Thcrapc^jtic Use.
Rlppoldsau, BiBck Korcst
Homburs, near Frankfort...
Elster. Saxony
Licbenstcin, North Gcrmony
1,886
1,«5
911
900
600
1,614
1,293
1,000
1,U3
5,404
1,463
■12
■10
■03
■08
•08
■OS
■07
■07
■07
•06
■04
■03
■06
■OS
■01
■It
For Bnieraic corditiona; laxative.
Po. do. do.
Do. do. do.
Do.; mach of a ladles^ bath.
Do.
Do.; laxative; a ladles' balh.
Do. do. do.
Do.
Do.
Do.; laxative.
Do.; sought for its air.
Do.
Do.
Do.
Do.:dc5cientincarbonicacid
Bocklet, near KIsslngcn
Grlesbach, Black Forest
Franzcnsbad. Bohemia
s "^""bcIcIutti
Pctcrsthal, Black Forest
St Moiltz. Encadlne, )
Switecrljnd >
Forgcs-les-Eaux, France
La Malou, Hcrault, )
Franco (temp. SS*) f
Rccoaro, North Italy
Tunbridgo Wells, England...
Ilu-pralt SjiilnK, Harro-\
pat« (chloride) )
MINERAL WATERS
435
fhl&djarant in tha strong StaKl Quelle of Homburg and in the
Putnam Well at Saratoga. A wliole category of female complaints is
treated successfully witn these waters. Indeed anaemia Irom any
fiource, as after fever or throut^h loss of blood, and enlargements of
the spleen, are benefited by tnem. The stimulating action of the
copious supply of carbonic acid in steel baths is a very important
adjuvant; no one now believes in direct absorpttion of iron from the
bath. Iron waters are scarcely ever thermal. They are extremely
common in all countries, — frequently along with sulphuretted
hytirogen in bogs, and near coal -measures. But such springs and
non-carbonated wells generally are weak, and not now held in much
esteem.
It may be added that some of the strongest known iron wells are
tulphaied or aluminaied. They arG styptic and astringent, and can
only be used diluted. They are sometimes useful as an application
to mcers and sores. Such springs have often been brought into notice,
but never retain their popularity. They are known m the Isle of
Wight, in Wales, in Scotland, as well as in Elba, &c. ; and of late
years the Bedford Alum and Oak Orchard Springs, U.S., Ijave been
brought into notice, the latter containing 10 grains of froo sulphuric
acid in the pint. All such springs have been considered useful in
scrofula, anaemiaj and chronic diarrhoeas.
Sulphur Springs. — Waters having the odour of hydrosulphuric
aiid, however slightly, are usually called sulphur ones. They owe
their smell sometiines to the presence of the free acid, sometimes
to sulphides of sodium, calcium, or magnesia, and sometimes to
both. Hydrosulphuric acid is absorbed more freely by cold than by
hot water, and is therefore most abundant in cold springs. The
sulphides decompose and give off the gas. Most of these springs
occur near coal or shale measures, or strata containing fossils, or in
moors and in places generally where organic matter is present in
the soil or strata. Many of them contain so little mineral impreg-
nation that they might as well be classed among the indifferent
or earthy waters. One group contains a considerable amount of
chloride of sodium, another ot sulphate of lime, while a third has
littlo mineral impregnation, but contains sulphides.
Hydi'osulphuric acid is a strong poison, and its action on the
system has been pretty well ascertained. It has been assumed that
the gas in mineral waters acts similarly, though in a modified
degree ; but there is next to nothing absolutely kno^vn of the
action of the small quantities of the gas that arc present in mineral
waters, and which certainly have no toxic effect. It has been
assumed that this gas has some special action on the portal system
and so on the liver. On the connexion of metallic poisoning
with the liver has been founded the idea that sulphur waters are
useful in metallic intoxication. Drinking large quantities of these
waters, especially of such as contain sulphates or chlorides of
sodium or magnesia, combined with hot baths and exercLso, may
help to break up albuminates, but there is no proof of the action
of the sulphur.
For similar reasons, and primarily to counteract mercurial poison,
sulphur waters have been considered useful in syphilis. But it
may be well to remember that at most baths mercury is used along
with them. No doubt they are frequently, like other warm' waters,
useful in bringing out old eruptions, acting in this way as a test
for syphilitic poison, and in indicating the treatment that may be
Table VII. — Cold Sulphur Spring
pKSd '»^f,''^
Water.
Eilaan. Schaumburg-Llppe ' 42-3
Molnberg, Llppe-Dctmold ., 23-1
Gumigel, Switzerland (3G00 ft.) I 15'1
Lcuk, do. (3593 It.). „ .i 44-5
Challes, Savoy (000 ft.)
Enghieii. near Paris
Uriago. Isfero, France (1500 ft.) 7-3i
Uan'ogatc, England
SlrathpctTer. Scotland
lilsdunvarna, CJare, Ireland
Table VIII. — Warm Sulphur Springs.
locollly.
Height
In Feet.
Temp.
• Fabr.
Sulphide
of Sodium.
Jlydrosul-
ptiuric Acid
absorbed iu
Water.
s:4
1,060
1,350
500
705
2,000
4,100
810
3,254
2,400
131-140
D5-115
80-02
92-113
110
108 5
135-5
113
87-147
71-134
00-5
126
•01
•052
;;;
'■07
•04'
•01
•02
•02
■3
2-5
37-3
3^5
42-6
27-2
"Bardgcs. dq,
C&uteret^ * "'' do
Eaux Bonnea do
Aicheim, Marcla. Spain
TMulred. Sulphur watera^both hot and cold, are used in gout and
rheumatism, m dyape|isia, in hepatic and cutaneous affections ; and
of late years inhalation of them has been popular in phthisis and
in laryngeal affections. They have long been popular remedies in
cutaneous affections. Wlule so much doubt has been cast on the
action of the sulphur of these waters, it may be admitted that the
sulphides are probably decomposed in the stomach and hydrosul-
phuric acid generated. That gas is probably a slight stimulant
to the intestine. What hydrosulphuric acid reaches the blood ia
ehmmated by the lungs. There seems to be no doubt that the gas
is absorbed in small quantities by the skin.
It is in sulphur -Boaters chiefly that glairin and baregin occur.
This peculiar organic substance has been found both in American and
in European springs. Cold sulphur springs are very widely diffused
throughout the world. Thermal ones are not so common. Per-
haps the largest though not the strongest group of the latter is to
be found in the Pyrenees. We may remark again how very little
hydrosulphuric acid there is in many of the most favourite sulphur
springs, including the very popular White Sulphur ones of Virginia.
There seems to be something peculiarly unsatisfactory in the
analysis of sulphur waters, and there has been difficulty in construct-
ing the following imperfect tables.
Some of the most powerful cold wells are those of Challes (with its
very peculiar water), Leuk, and Harrogate. Uriage has a very.largo
amount of chloride of sodium in its springs. Coki sulphur waters
are on the whole more used in liver and indigestion than warm
ones. The general effects of warm sulphur waters differ so littlo
at the various baths as to make it difficult to mention anything
special to particular localities. Schinznach has a reputation in
skin complaints, Cauterets, Eaux Bonnes, and Challes in laryngeal
affections, the two Aixes, Luclion, and Archena in syphilis.
Alkaline Waters are such as contain carbonate (chiefly bicarbon-
ate) of soda, along with an excess of carbonic acid. Of the action of
those carbonates it is known that when taken into the stomach
they are neutralized by the gastric juice, and converted into chloride
of sodium. On their introduction into the stomach they produce
an increased flow of gastric juice. If given during or immediately
after meals in any quantity, they impede digestion. They slightly
increase peristaltic action, but only feebly, unless assisted by other
salts. They act slightly as diuretics. Of the connexion between
the biliary system and alkalies, which undoubtedly exists, not much
is known with certainty. The alkalization of the blood by them is
assumed by many, but not proved. It is very doubtful whether
they reduce the quantity of fibrinc in the blood, and thus induce a
Table IX. — Alkaline Waters.
Class l.Simpfe Alkalit
Vala, South France
Bllin, Bohemia
Vichy, France (105" F.) ,
Neucnahr, Hhlneland (92*-97* F.),
La Malou, France (37* F.)
VIdago, Portugal
Therapeutic Uses.
(, diabetes.
Do.
Do.
Mucous catarrh; diabetes specially,
f Do. ; sedative effect on nervous
I system.
j Do., gout, urinary affections — "TJie
( Portdgueso Vicliy."
i If. — With Chloride of Sodium vartiin^ /ront 4^3 to I in amount.
Locality.
Luhatschowltz, Moravia..
Tcinnistcin, Rhine Valley.
Fms, Nassau
Ischia, Italy
Royat, Auvergne
Mont Dore, do
Bourboule, do
Height
in Feet
Temp.
• Fahr.
Cavb.
Soda.
1,000
84
2-5
85-116
2^0
npt(yl70
2 0
1,400
80-35
■ •3
3,300
100-114
2,800
107-125
Therapeutic Uses.
J Springs rich both in carb.
SpL'cially rheiimatlBm
and ftmale complaintB.
I Do. and some skin
I affections.
? Asthma; chronic larj'"'
\ gitis.
J Scrofula, rachitis, cuta-
1 ncoua affcciiona.
Tamap, Lower Engadin*;
Ciilsbad, Bohemia (lil'-lGl' 1
Do.; spccifll
Do.; spL'ciaDy a ladies' bath.
i rowLTfcl action on aidomEnal
436
MINERAL WATERS
lowered stato of the sjstcm, or whether they have auy direct tend-
ency to combine with fat and carry off a portion of superfluous
adipose tissue. Their excess of carbonic acid, through its action on
the stomach, favours the operation of alkaline waters. They have
been classed as follows: — (I.) siniitle alkaliues, where carbonate of
soda is the main agent ; (II.) waters containing in addition some
chloride of sodium ; (ill. ) waters containing sulphates of soda or of
magnesia. All these classes may be said to be used in gout, lithi-
asis, affections of the liver, catarrh, and obstructions of the gall
ducts, in dyspepsia, chronic catarrh of the stomach, and diarrhcea,
in obesity, and in diabetes. Some of the waters of the second class
are supposed to influence bronchial catarrhs and incipient phthisis,
wliile tlie more powerful sulphated waters of the third class are
especially useful in catarrh of the stomach, and in aflections of the
biliary organs ; of thoee only one of importance (Carlsbad) is ther-
mal. The rival cold waters of Tarasp contain twice as much car-
bonate of soda. The cold ones are chiefly used internally, the
thermal ones both internally and externally. The latter, besides
acting as warm water, slightly stimulate the skin when the car-
bouic acid is abundant, and the carbonate of soda has some slight
detergent effect on the cutaneous surface like soap. These waters
are unknown in England. They are most abundant in countries of
extinct volcanoes.
Classes I. and II. of alkaline waters may be said to have a sub-
variety in acidulated springs or carbonated waters, in which the
quantity of salts is very small, that of carbonic acid large. These
table waters are readily drunk at meals. They have of late years
been so widely exported as to bo within the reach almost of every
one. Their practical importance in aiding digestion is in reality
much greater than one could expect from their scanty mineraliza-
tion. They are drunk by the country people, and also largely ex-
ported and imitated. "^'I'^y ?ve very abundant on the Continent,
and, although some of tl'o best-known ones enumerated below are
German an I French, tluy f-ie common in Italy and elsewhere:—
Heppingeii, Roisdorf, Landskro, Apollinaris, Selters, Brlickenau,
Gicsliiibel, all German ; St Galmier, Pougues, Chateldon, French.
Associated with Class III. is that of the stToHQly snlpliatcd waters
known in Germany as bitter or purging waters, which liave of late
deservedly come into use as purgative agents. They aro almost
wanting in France and in America, and there are no very good ones
in England. The chief supply is from Bohemia and Hungary. The
numerous waters of Ofen are the best-known, and some of them are
stronger than the Kunyadi, of which an analysis has been given in
Table I. They are eafsily imitated. Some of the best-known are
Ofen, Ptillna, "Saidschiitz, Friedrichshall, BirmerstolF, Kissingen.
Two otlier classes of waters demand a few words of notice. The
French have much faith in the presence of minute quantities of
areeuic in some of their springs, and ti-ace arsenical effects in those
who drink them, and some French authors have established a class
of arsenical waters. Bourboule in Auvergne is the strongest of
them, and is sai<l to contain i^jth of a grain of arseniato of soda
in 7 ounces of water. Baden-Baden, according to Bunsen's latest
analysis, has a right to be considered an arsenical watei-. It is,
however, extremely doubtful whether the small amounts of ar-
seniate of soda which have been detected, accompanied as they are
by preponderating amounts of other salts, have any actual opera-
tion on the system. The following aro among the most noted
springs : — Bourboule, Mont Dore, Uoyat, Salies (Bigorres), Plom-
bi^res, Baden-Baden.
Of late years lithium has been discovered in the waters of Baden-
Baden ; and various other places boast of the amount of that sub-
stance in their springs. Indeed a new bath has been established at
Assmannshausen on the Khino in consequence of the discovery of
a weak alkaline spring containing some lithium. Not very much
is kno\\'n of the action of lithium in ordinary medicine, and it un-
doubtedly docs not exist in medicinal doses even in the strongest
springs. Among these springs aro those of Baden-Baden, Assmanns-
hausen, Elster, Royat, Ballston Spa, and Saratoga (U.S.).
American Mineral Waters. — Tho number of springs in the
United States and Canada to which public attention has been
called on account of their supposed tncrapeuttc virtues is very
large, amounting in all to more than three hundred. Of tliis number
comparatively few arc in Canada, and of these not m'^re than six (St
Catharines, Caledonia, Plantagcnet, Caxton, Charlottesville, and
Sandwich) have attained general celebrity. The first thrtfe belong
to the saline class, the Caxton is alkaline-saline, and the last two aro
sulphur waters. Tho St Catherines is remarkable for the very large
amounts of sodium, calcium, and magnesium cliloridcs which it
contains, its total salts (450 grains in the pint) being more than
throe times the quantity contained in tho brine-baths of Kreuz-
nach in Prussia. The Cliarlottesvillo and Sandwicli si)rings likewise
surpass tho noted sulphur-waters of Europe in their excessive per-
centages of sulphuretted ]iydro"cn, the former con tainingmorotlian
3 and the latter 472 cubic inches of this gas in the pint.
TIte mineral springs in tho United States ore very unequally dis-
tribiitcd, by far the larger number of those which aro in high
medical repute occurring along the Aj>palachiau chain of mountains,
and more especially on or near this chain where it passes through the
States of Virginia, "West Virginia, and New York. The Devonian
and Silurian formations which overlie the Eozoic rocks along tlie
course of the Appalaghian chain have been greatly fissured — the
faulting of the strata being in some places of enormous magnitude
— by the series of upheavals which gave rise to the many parallel
mountain ridges of the Appalachians. In many places the springs
occur directly along the lines of faidt. The various classes of
mineral waters are likewise very unequally represented, the alkaline
springs, and those containing Glauber and Epsom salts, being much
inferior to their European representatives. On the other hand, the
very numeroils and abundant springs of Saratoga compare very
favourably with the Selters and similar saline waters, and amon^
the many American clialybeate springs the subclass represented
by tho Rockbridge Alum is unequalled in regard to the very large
percentages of alumina and sulphuric acid which it contains.
Besides its greater amount Of mineral constituents (135 grains per
pint), the Ballston spring surpasses the similar saline waters of
Homburg, Kissingen, Wiesbaden, and Selters in its percentage of
carbonic acid (53 cubic inches). It is also remarkable for the very
largo proportion of carbonate of lichia, amounting to 0701 grains.
Thermal spring are specially numerous in the territories west of
tho Mississippi and in California. Those in the east mostly occur
in Virginia along the southern portion of the Appalachian chain ;
in the middle and New England States Lebanon is the only im-
portant thermal spring. Subjoined is a list of thirty American
springs, the design being to represent as many of the more noted
sjias as possible, while at the same time enumerating the best repre-
sentatives of the classes and subclasses into wliicli mineral waters
are divided according to the German method of classification.
Designation ai'd Locality.
'Lebanon, CoIumWa Co., N.Y. (TS° F.).
IleaUng, Bath Co., Va. (SS° F.)
Worm, Bath Co., Va. (98" F.)..
Hot, Bath Co., Va. (110' F.) .,
Hot, Garliinil Co., Ark. (ft3'-150" F.)...,
Gettysburg, Adams Co., Pcnn
Sweet, 5Ionroc Co., W. Vn. {74" F.)...
ELtliesdn, "Waukcslia Co., Wis...
WhUc Snlphur, Grccnbiuir Co.. Va. ..
Salt Sulphur, Monroe Co., W. Va
> Bedford, Bedford Co., Pcnn
fSt Catherines, Ontario, Canada
Caledonia, Ontario, Canada.
Hathome, Saratoga, X.Y
Ballston, Suratoga Co.. N.V
Oak-Orchard Acid, Gl'i
:Co.,N.Y..
Rawley, Rockinglmm Co., Va..
Cooper's Well, Hinds Co., Miss...
life
/Sladon, Choctaw Co., AIn. (carbon- >
nted nlkalliic) f
I Congress, S;inta Clurti Co., Cul. [
\ (snlinc alkn'iiiO J
St Louis. Gratiot Co., Mtch. (>Implc (
V allialinc) f
Therapeutic Application
C Scrofulous ulcers and ophthal-
J niia,oza.'na,cliionic dianh
1 and dyscntciy, secondary
( and tertiaiy syphilis.
^Chronic and subacute rlicnina-
■< tism, gout, neuralgia, neph'
( rltic and calculous disca&'cs.
{Chronic rheumatism, gout,
diseases of liver, neuralgia,
contractions of joints.
(Dartrous diseases of skin,
1 fuuct ional di&casesof uterus,
j clironic mercurial and lc;id
( poisoning.
] Calcuhis, frniTcl, catarrh of
J stomach or bladder.dysiicpsls,
J Gravel, dyspepsia (diuietJc,
\ diaphorciic).
Nturalcia (rcstomtivc).
Purgative, diuretic.
( Diabetes mcllltus, gravel, in-
■i flamniaiton uf bladdor.dropsy,
( nJbuinlnuria (diuivtic).
" and altcrativo.
Do.
do.
iDai-lrous skin diseases, dis-
eases of the bladdur, jaun-
dice, dy^pipfla.
Do.; scrofula and syphil:
{Anaimio, pavel calculus
(strongly diuretic).
1 Rheumatism, gout, scrofula.
■alpin.
Ilhcuniitiism. gout.
(Dyspepsia, jaundice, nbdoml-
1 nai plethora.
Do. do. do.
(Ulcci*5, diseases of tho skin
) passive h.-cmoiThngi-s, ulonii
) diairlicra(liaslOgr.ilnsoffm
Hlpluiiic ncid Jn Uic pint).
Scrofula, chronic dlnnhc
(Anrenila, chloi-osls, ch
{ dlairhoia, djopsy.
Jiibliographtj.—l. i'ivrma.n : E. Osnnii. PurstfUmig da' /Irilqiieflm Eiiropas,
8 vols., Berlin, 19.10-43 ; J. Soecen. Ilaudbuchder //, ilquellcnte/uY, Vienna. lbG2;
B. .M. Lcrscli, J/pdrochemie, 1S70, and many other works; Hclfft, Handbuch d.
Bahitothcrapie, 8lh cd., Berlin. IST4 ; VHleiitliier, llandbuch d. ffalNfcthera/u'e,
Berlin, 1S76; L. Lchmann. Odder v. Prunnen Lcht, Bonn, IR'T ; J. Uraun,
Sffiftm. Lfhrbuth d. Balneotherapie, 4th cd., by Fromm, BerMn, ISSO; O. Lclch-
tcnsicrn. Balneotherapir, Leiitsle. ISSO. 2. French: Dtrtionnairc Jtt E.tux
minn-alts. Ac. by MM. Durond- Fardel. .Vc. 2 vols., Paris. 18C0; ,L Lcfnrt, Traits dt
Cheinte Jtydrolologigue^ 2d cd., Paris, lbV3 ; C James. Gnidt Pi-afiQae aiix Z'anx
M I N — M I N
437
mtnerare$, Paris (many editions) ; Mactf, Guide aux ViVts ^Eatix, Aft. Paris,
18^1; Jounne and L« Pileur,£«j Sdifif (f furore, raris. 3. Swiss; Meyer Ahrens,
IIttl<juetten dtr Ikhireitt^ ZUrich, 1&G7 ; GscU Fcis, Die Bader urtd Kurorle der
Schacilt, ZUrlcll, 1S80. 4. Italian ; G. Jcrvis, GttiJa alle Acgue Minerati
d'ltalia. Tuiin, 1870, Jcc; E. F. Horltss, Die ffei/quetten und Kurluder Jlalieru,
Berlin, 1848. 5. Spanish : Rubio, Tralado de lai Fuenteg Minaalei de Etpana,
Uadrid, 1853; Don J. de Antelo y Sanchez has recently published a work on Sp<>nish
waters, ti. English : T. Short, Uittory o/ the Miiitrat Waters, London, 1734; J.
Rutty, ifethodicai Synopsis of Mineral Waters, London, 1757; Granville, Spas of
England, 1S41; E. Lee, itiiieral Springs of England, London, 1841; J. Macpher-
son. Our Baths and Wells, 1871 ; Id^ Baths and Wells of Europe, 1873; and H.
AVeber's EnRlish edition o[ Braun, London, 1875. A great portion of the literature
Is to be found in monographs on paitlcular plaees. 7. American : J. Bell, The
ilineral and Thermal Springs of the United Slates and Canada, 1855; Moorman,
The Mineral Waters of the United Stales and Canada, 18C7; Chandler, Leelnre
on Water, 1871 ; Walton, TAs Mineral Springs of the United " ales and Canada.
1875. (J. M.— A. K. L.)
MINERVA (i.e,, menes^a, endowed irith mind) was the
Roman goddess who presided over all handicrafts, inven-
tions, arts, and sciences. She %.as probably an Etruscan
deity, but her character was modified on Roman soil through
lier identification with the Greek Pallas Athena (see
Athena). No legend of her birth is recorded ; the Roman
deities .were abstractions, not distinct persons with an
indiWdual history. Her chief worship in Rome was in the
temple built by Tarquin on the Capitol, where she was
worshipped side by side with Jupiter and Juno. This
foundation may be assigned to Etruscan influence. She
had also an old temple on the Aventine, which was a regular
meeting-place for dramatic poets and actors. The dedi-
cation day of the temple and birthday of the goddess
Avas March 19, and this day was the great festival of
Minerva, called quinquaints because it fell on the fifth
day after the Ides. The number five was sacred to the
goddess. All the schools had holidays at this time, and
the pupils on reassembling brought a fee (minerval) to the
teachers. In every house also the quinquatrus was a
holiday, for Minerva was patron of the women's weaving
and spinning and the workmen's craft. At a later time
the festival was extended over five day.s, and games were
celebrated. This feature is evidently due to the Grsecizing
conception of Minerva as the goddess of war. To this same
Groecizing tendency we must attribute the lectistemium
to Minerva and Neptune conjointly after the battle of the
Trasimene Lake. The 23d had always been the day of
the tubitusirinm, or purification of the trumpets, so that the
ceremony came to be on the last day of Jlinerva's festival.
Trumpets were used in many religious ceremonies ; and
it is very doubtful whether the iuhihtstrium was really con-
nected with Jlinerva. There was another temple of Minerva
on the Cotlian HiU, and a festival called the lesser nmnr
^uatrus was celebrated there on June 13-15, chiefly bv the
flute-players.
Minerv.t of the Cxlian temple was callod Capta; June 19 was
the foniulatiou day ol' tins temple and tlio birtliday of the goddess.
Tltc iialladium, au archaic image of Pallas, was broujlit fiom Troy
to Laviiiiuni, auU tUeuco to Rome by the family of the Kaiitii ; it
w.as preserved iu the tcmpio of Vesta as a pledge of tlie safety of
tlic city. Tliere are some traces of an identilication of Minerva with
tlic Italian goddess ICerio, wife of JIarsj it is probable Ihat March
ID was originally a feast of Jlars.
Decide:" Prcllcr, /lUm. Mutli., and irartnnc, lielig J. ltSiner,&c., sec Jorda
Epltem, Epigraph., i. 233; Moinmscn, C. /. i., I. S38: I'acacr, Jihefti. J/us., xsx.
MINGRELIA, a former principality of Transcaucasia,
which became subject to Russia in 1804, and since li?67
has constituted three circles of the government of Kutais —
Lotchgum, Seuakh, and Zugdidi. The country corresjionds
to tlie ancient Colchis; and Izgaur or Iskuriah on the Black
Sea coast, which was the capital during the period of
Jlingreliaii independence under the Dadian dynasty, is to
be identified with the ancient DIoscurias, a colony of
Miletu.-*. The Mingrelians (still ahnost exclusively confined
to the Mingreliau territory, and numbering 197,000) are
^osely akin to the Georgians See Caucasus, vol. v. p.
257, and (>'EonnT.i.
MIXLiTURE is u term \vliich by common usage has
come to be applied to two different branches of painting.
Derived from the Latin word minium, the red pigment
used in the primitive decoration of MSS., in the first place
it ia the technical word employed to describe a painting in
a MS. ; and, from the fact of such pictures being executed
on a reduced scale, it has its secondary and modem signifi-
cation of a small, or miniature, portrait. In the latter sense
it belongs to the general subject of painting. Here it is
proposed to trace the development of the miniature in MSSl
of the different schoob of Europe.
The rise of the art of Illumination, in which the
miniature plays so important a part, has been described
under that heading ; and something has been said in that
place about the earliest extant specimens of miniature
painting. Unfortunately we cannot with any certainty
reach farther back than the 4th century for the most
ancient of them ; and all remaining examples between that
period and the 7th century iu Greek and Latin MSS.
can be counted on the fingers. The two famous codices of
Virgil in the Vatican Library stand pre-eminent as the
most ancient Latin MSS. decorated with paintings. The
miniatures in the first of them, the Codejc Smnaniti-,
are large and roughly yet boldly executed paintings, which
have no pretension to beauty, and are simply illustra-
tions ; but they are as old as the 4th century, and are
of the highest value in enabling us to appreciate the
debased style to which classical art had descended, and
which no doubt was more largely employed than we might
think. The second MS., the Sckedx Vatkanix, which may
also be assigned to the 4th century, is far more artistic
and retains a good deal of the grace of classic art. Of
the same kind, but of rather later date, are the fragments
of the Iliad in the Ambrosian Library at Milan, the
miniatures of which are generally of exceUeat design.
Next comes the Dioscorides of the Imperial Library at
Vienna, with its semiclassical portrait-miniatures executed
at the beginning of the 6th century. Of a rather later
period are the paintings which illustrate the Greek MS.
of Genesis in the same library. A far finer and older MS.
of the same book of the Pentateuch once esusted in the
Cottonian Library, but was almost totally destroyed by
fire. The few fragments of the miniatures which once
filled this volume, and which were of the 5th century, are
sufficient to show what excellent work could be done in the
capital o( the eastern empire, from whence the MSS. most
probably came. The late interesting discovery of an illus-
trated SIS. of the Gospels in Greek, of the latter part of
the 6th century, at Rossano in southern Italy, adds another
number to our scanty list of early volumes of this class,
which is closed by the Latin Pentateuch in the library of
the earl of Ashburnham. This last JIS., however, is not
older than the 7th century. It was executed in Italy,
and is adorned with many large miniature.", not of high
artistic merit, but of great interest foi the history of
painting and of costume.
Coeval with the MSS. which have just been enumerated
are the beautiful mosaics and wall-paintings which are
seen at Rome, Ravenna, and in other parts of Italy, serving
as standards of comparison and carrying on the history of
art where MSS. fail us. The strong and ever-increasing
P.yzantiue element which appears in these works prepares
us to find the predominance of the same influence when we
again pick up the broken thread of the history of miniature
painting. We may then, at this point, turn for a moment
to the east of Europe and state briefly what remains of
Greek art in MSS. Of Greek miniaUires there are still
many fine examples extant, but, excepting those which
have been noticed above, there are few which are earlier
than the 11th century. At this period the miniatiue
appears in the set form which it retained for the next two
or three hundred years; and the connexion between its
438
M J ii) I A T U H E
style and that of -the mosaiSs is too evident for us to be at
i loss to explain the course of development. The figure
Ira wing is delicate, but rather exaggerated in length; the
jolours are brilliant; and the whole effect is heightened by
flittering backgrounds of gold. In some few instances,
aowever, the Greek artist breaks away from conventionalism,
and, especially when potirtraying the divine features of the
Saviour or some subject which deeply stirs his feelings, he
surprises us with the noble dignity with which he invests
his figures. Minuteness also caught the fancy of these
Byzantine miniaturists ; and there still remain MSS., such
as Psalters and saints' lives, adorned throughout with
delicate little dravrings of great symmetry and beauty.
rhe ornamentation which was employed in Greek MSS.
in the period of which we are speaking, either as frames
tor miniatures or as borders or head-pieces, is designed
Bvidently after Eastern types, and has 'more than an
ascidental likeness to the patterns which are seen in the
tapestries tmd prayer-carpels of Persia. After the 13th
century decadence sets in, and we need not foUow the
course of Byzantine art in MSS. farther than to notice that
immediately from it sprang such national styles as those
of .Russia, Bulgaria, and modern Greece.
Meanwhile, in the West, under the fostering care of
Charlemagne, arose a great school of deccfation in MSS.,
which at the close of the 8th and beginning of the 9th
century were multiplied and enriched vfith all the splendour
that colours and gilding could give to them. But the
books thus ornamented were almost always copies of the
Gospels, or Bibles, or chui-ch service books, which afforded
little scope for invention. Hence among the miniatures of
this period we have an endless repetition of portraits of
the evangelists, drawn, for the most part, in a lifeless way
aft* Byzantine traditions, and degenerating, as time passes,
into positive ugliness. The few miniatures of other descrip-
tions, such as Biblical illustrations, show no "great merit,
and a half-barbaric splendour was generally prefeiTed to
artistic effect. But an exception must be made in regard
to the style of drawing found in the MS. Jcnown, on
account of its present resting-place, as the Utrecht Psalter.
This volume is filled from beginning to end with delicately
drawn pen iUustratious, designed and execufsd with a
facility which, compared with the mechanical and clumsy
drawing of other Continental MSS. of the period, is astonish-
ing. And these drawings are of particular interest for us,'
as they are of the style which was adopted in England and
which gives to Anglo-Saxon art its distinctive aspect.
Executed about the year 800 or early in the 9th century,
and probably in the north of France, the vohimo was soon
brought to England, where, however, MSS. of the same
kind, it may be a.ssumed, had long" before been intro-
duced. The light " fluttering " outlines of the drapery and
other details of the tlrawings seem to suggest that the
original models were derived directly from Roman life, and
perhaps partly copied from sculpture; but those models
must have gone through many modifications before passing
into the style of the drawings of the Psalter. That the
MS. was copied from an older one there can be scarcely a
doubt ; and it is not impossible that the original archetype
may date back some centuries earlier. May not MSS.
which St Augustine and his successors brought from Rome
have contained drawings of the same kind ') This style of
drawing was, at all events, adopted and became nationalized
in England ; but it had there a rival in the Irish school of
ornamentation, introduced from the north of the island.
The early civilization of Ireland placed her in the van of art
development in these islands. The wonderfully intricate
interlaced designs which render Irish MSS. of the 7th
and 8th centuries such marvels of exact worlcnianship
derive their origin, in all proljability, from the metal- work
of earlier ages. . Bat, apart from ornamentation, the Irish
miniatures of saints and evangelists are extraordinary and
grotesque instances of purely mechanical drawing, which
cause us to wonder how the same eyes and hands which
assisted in the creation of such beautiful specimens of pure
ornament could tolerate such caricatures of the human
shape. The explanation is perhaps to be foimd in super-
stitious regard for tradition. ' This style of art was carried
by the monks to lona and thence to Lindisfame, where was
founded the school which produced, in the 8th and 9th
centuries, the richly ornamented codices of Durham. WhUe,
then, Byzantine models were copied on the Continent, the
free drawing introduced from the south and the intricate
ornamentation brought in from the north were practised in
England ; bift the free drawing, with its accompanying
decoration copied from foliage, and gradually developing
into beautiful borders harmoniously coloured, gained the
day, and lasted dawn to the time of the Norman Conquest.
The one great fault of this latter style of drawing strikes
the ej'e at the first glance. This is the inordinate length
of limb with which the human figures are endowed. But
this blemish is forgotten when one comes to appreciate the
many points of merit in the designs.
In Italj', after a long period of inactivity, two very-
different styles' of decoration of MSS. sprang into existence.
The first of these was' that of the Eombardic school, which
is distinguished by intricate patterns and bright colourisg.
The large initial letters which are found in the MSS. of
the 11th and 12th centuries, the best period of this
style, are often a perfect maze of interlaced bands and animal
forms, and are extremely handsome and effective. Figure
drawing, however, seems to have been but little practised
by the Lombardic artists, but such as there is appears on
a broad scale and well executed. In the collections of
Monte Cassino are some of the best examples of this
school. In the second style which developed in Italy tlie
Byzantine influence is at first most marked. Indeed,
among its early specimens of the 13th century are
some which might pass for the work of Greek artists. ' But
the genius of the Italians soon assimilated the foreign
element, and produced a national school which spread
throughout the peninsula and afterwards extended its
influence to southern France and Spain. It is, however,
remarkable that in a country which produced such fine
pictures and wall-paintings at an early date there is com-
paratively little miniature painting in cou'cemporary !MS3.
A curious and earlj' instance of this kind of art occurs
in. a MS. in the British Museum, written and orna-
mented with a series of miniatures at Winchester, in the
12th century, in which are two paintings T\'hich are
purptxrlj^lian and of more than ordinary excellence.
In'the majority of the extant Italian miniatures of the
14th century the influence of the great artists of the
Florentine school is manifest. The peculiar treatment oi
flesh tints, painted in body colour over a foundation of
olive-green, and the peculiar vermilion and other colours
which need be but once seen to be ever afterwards recog-
nized as belonging to this school, a're constantly present.
The figures are generally rather shortened and the drapery
carried in straiglit folds, vei-y different characteristics from
the swaying figures and flowing drapery of the English and
French artists of the same period. .The ornamentation
which accompanied this stylo of miniature generally
consi.sts of hoaNy scrolls and foliated or feather-like
pendants from the initial letters, with spots of gold set
here and there in the border. There are also extant soma
examples of a most beautiful kind of ornamentation which
appears to have originated in central Italy, and which
seems to partake of the qualities of both the styles of
Italian art of which we have been erionkinir, combining
Jil 1 N 1 A J L' li E
439
ine draivjau; of the J^'lorentiue school with a lighter coloui-
•a^whicfi'inay have been suggested by the Lombardic.
^Of native Spanish miniature art little can be said. In
the Visigothic MSS. of the early Middle Ages there is no
ornament beyond roughly coloured initial letters and some
barbaric figure drawing. A little later, however, we get
some indication of national peculiarities in the MSS. of
the 10th, 11th, and 12th centuries. Here there appear
miniatures, stiff and rude in their drawing, but exhibiting
the unmistakable Spanish predilection for sombre colours,
' — dusky reds and yellows and even black entering largely
into the compositions.
iThe materials at our disposal of the 10th, 11th, ana
12th centuries show the gradual development in France
and western Germany of a fine free-hand drawing which
was ' encouraged by the proportionately increasing size
of books. Both in outline and colour the fully de-
veloped miniatures of the 12th century are on a grand
scale ; and initial letters formed of scrolls and interlacings
assume the same proportions. The figure drawing of this
time is frequently of great excellence, the limbs being well-
proportioned ; care is also bestowed upon the arrangement
of the drapery, which is made to follow the shape and. as
it were, to cling to the body.
But the great revulsion from the broad effects and bold
grandeur of the 1 2th century to the exact details and careful
finish of the 13th century is nowhere more striking than
in miniature painting in MSS. With the opening of the
new period we enter on a new world of ideas. Large
books generally disappear to give place to smaller ones.;
minute writing supersedes the large hand ; and miniatures
appear in circumscribed spaces in the interior of initial
letters. The combination of the miniature mth the initial
brings it into close connexion with the ornamental border,
which develops pm-i passu with the growth of the minia-
ture and by degrees assumes the same national and
distinctive characteristics. Burnished gold was now also
freely used, tending to give the miniature a more decorative
character than formerly. In England, northern France,
and the Netherlands the style of miniature jjainting of
this period was much the same in character ; and it is
often difficult to decide from which of these countries a
MS. is derived. English work, however, may be often
distinguished by its lighter colouring, while deeper and
more brilliant hues and a peculiar reddish or copper tinge
in the gold marks French origin. The drawing of the
Flemish artists was scarcely so good, the outlines being
frequently heavy and the colours rather dull. Of the
Rhenish or Cologne school examples are more scarce ; but
they generally show greater contrasts in the colours,
which, tlioi\gh brilliant, are not so pleasing. As the
century advanced, and particidavly at its close, national
distinctions became more defined. English artists paid
more attention to gracefid drawing and depended less
upon colour. In some of their- best productio^is they are
satisfied with slightly tinting the figures, finding room in
the backgrounds for display of bi iUiant colours and gilding.
In France the drawing, though exact, is hardly so graceful,
and colour plays a more important part. ■ From the 13th
to the middle of the loth century great decorative effect
is obtained by the introduction of diapered or other highljre
ornamented backgrounds. ' Of landscape, properly so called,
there is but little, a conventional hill or tree being often
taken as sufficient indication. Borders begin in the 13th
"cntury in ;lic form of simple pendants from the initial
•fetters, terminating in simple buds or cusps. '= But once
arrived f.iiiiy in tlie Uth century, a rapid development in
all parts of the decoration of ilSS. takes place. There is
"icatcr^freedom in the drawing; the borders begin to throw
onrmanches and the bud expands into leaf, t This is the best
peri'jd of English miniature painting, many of the fine MSS.
of this century which are preserved in the public libraries
bearing witness to the skill and delicate touch of native
artists. In France the decoration of JISS. received a great
impetus from the patronage of King John and Charles V.,
of whose famous libraries many handsome volumes are still
to be seen; and later in the century the duke of Bern
carried on the same good work.
With regard to miniature art in Germany there are so
few examples to guide us that little can be said. Most of
them are rough in both drawing and colouring ; and in
the few remaining specimens of really good work foreign
influence is distinctly seen. In the west the art of France
and Flanders, and in the south that of Italy, are pre-
dominant. Perhaps the finest JIS. of this southern style
to be seen in England is a Fsalter belonging to
Lord Ashburnham, which was probably executed in the
Hth century at Prague, and is full of miniatures which
in drawing and colouring follow the Italian school.
When ve enter the 15th century we find great changes
in both the great English and French schools. In
England the graceful drawing of the previous century has
disappeared. At first, however, some beautiful examples of
purely native work were produced, and still remain to excite
our admiration. Probably the most perfect of these JISS.
are the Sherborne Missal belonging to the duke of Nortli-
umberland, and a very beautiful volume, a Book of Hour.s,
in the library of Lord Ashburnham. The care bestowed
upon the modelling of the features is particularly.noticeable
in English work of this period. In decoration the border
of the l-tth century had by this time grown to a solid frame
surrounding the page ; but now another form of most effec-
tive ornament was also used, consisting of twisted feather-
like scrolls brightly coloured and gilt. As the century
advanced native English work died out, and French and
then Flemish influence stepped in.
In France immense activity was shown all through the
loth century in the illumination and illustration of books
of all kinds, sacred and profane ; and it is in the MSS.
of that country, and, a httle later, in those of the Low
Countries, that we can most exactly watch the transition
from mediaeval to modern painting. Early in the century
there were executed in France some of the most famous
MSS. which have descended to us. In these the co/ourtng
is most brilliant, the figure drawing fairly exact; and the
landscape begins to develop. The border has grown from
the branching pendant to a framevork of golden sprays or
of conventional and realistic leafage and flowers. Towards
the middle of the century the diaper disappears for ever,
and the landscape is a recognized part of the miniature ;
but perspective is still at fault, and the mystery of the
horizon is not solved until the centivy is well advanced.
And now Flemish art, whi^ji had long lain dormant, sprang
into rivalry with its French sister, under the stimulus given
to it by the Van Eycks, and the struggle was carried on,
but unequally, through the rest of the century. Fi'ench
art gradually deteriorates ; the miniatures become flat and
hard ; nor are these defects compensated for by the
meretricious practice of heightening the colours by pro-
fusely touching them with gold. The Flemish artists, on
the other hand, went on improving in depth and softness
of colouring, and brought miniature painting to rare perfec-
tion. The borders also which they introduced gave scope
for the study of natural objects. Flowers, insects, birds,
and jewels were painted in detached groups on' a solid
framework of colour surrounding the page.
But if, as t!ie 1 5th century drew to its close, the Flemings
had outstripped their French rivals, they had now more
powerful antagonists to contend with._..^The ItaUans had
been.advancing jivith rapid strides towards .the glories o£
440
M I N— M I N
the Renaissance. Early in the century there arose a taste
tor older models. As, for their writing and a"fterwards
for their printing, they went back to the 11th and 12tli
centuries for their standards, so they adopted again the
interlacing designs of the Lorabardic school for their omar
ment, and produced beautiful borders of twining patterns
relieved by colour ; or they took natural objects for their
models, and painted borders of delicate flowers made still
more brilliant with clustering stars of gold. Later, they
drew from the ancient classical designs inspiration for the
wonderful borders of arabesques, medallions, grifiins, human
forms, antique objects, <fec., which they brought to such
perfection early in the next century. Their miniatures
rose to the rank of exquisitely finished pictures, and were
executed by some of the best artists working under the
patronage of such great houses as those of Sforza and
Medici.
Here then, having advanced to the threshold of the
domain of modem painting, we leave these two great
schools of miniaturists in possession of the west of Europe.
The Flemings had the wider field j they were wanderers
from home ; and their works are scattered through mtvij
lands, from England in the north to Spain in the south.
But Italian art had greater inherent strength, and will
always hold the first rank. To instance a few of the more
famous MSS. of this closing period of miniatvire painting :
the Breviary of Isabella the Catholic, in the British
Museum, is a masterpiece, of Flemish art produced In
Spain ; the Grimani Breviary at Venice is another fine
example of the same school. Some beautiful Italian
miniatures (executed for Leo X. and others) were in the
collection lately sold by the duke of Hamilton. The earl
of Ashburnham possesses a most delicately illuminated
Book of Hours written for Lorenzo dei Medici' by the
famous scribe Sinibaldo in 1485, as well as a MS. to which.
Perugino and his contemporaries contributed paintings.
And in one MS., a Book of Hours belonging to Mr Malcolm
of Poltalloch, are gathered some of the best miniatures
of both schools, viz., a series of exquisite paintings by
Milanese artists supplemented by later ones of the finest
Flemish type. (e. m. t.)
MINIMS. See Trahcis (St) of Paola, toL ix. p. 605.
MINING
THE art of mining consists of those processes by which
ixsefiJ minerals are obtained from the earth's crust.
This definition is ■nider than what is popularly known as
mining, for it includes not only underground excavations
but also open workings ; at the same time it excludes under-
ground workings which are simpfy used for passages, such
as railway tunnels and sewers, and galleries for military
purposes. We must remark also that the word " mine," or
its equivalent in other languages, varies in signification in
different countries on account of ' legal enactments or
decisions which define it. Thus, in France and Belgium,
the workings for mineral are classified by the law of 1810,
according to the nature of the substance wrought, into
mines, ininieres, et carrieres. In the United Kingdom, on
the contrary, it is the nature of the excavation which
decides the question for certain legislative purposes, and
the term mine is restricted to worldngs which are carried
on underground by artificial light. The consequence is
that what is merely an underground st£)ne quarry in
France becomes a true mine in England, whilst the open
workings for iron ore, such as exist in Northampton-
shire, would be true mines uniler the French law. It is
necessary, therefore, in an article on mining, to go beyond
the English legal definition of a mine,, and include the
methods of working minerals in excavations open to day-
light as well as in those which are purely subterracsan..
Furthermore, as it is customary for the miner to cleanse
his ore to a greater or less extent before selling it to the
smelter, we shall treat, under the head of mining, those
processes which are conunonly known as the dressing or
mechanical preparation of ores ; and, finally, a few remarks
will be made concerning legislation affecting mines in the
United Kingdom, accidents in mines, and the production
of the useful minerals in various parts of the globe.
The subject therefore will be dealt with as follows : —
1. Manner in which the useful minerals occur in the
earth's crust, viz., tabular deposits and masses ; faults or
dislocations.
2. Prospecting, or search for mineral.
3. Boring with rods an^l ropes ; diarnond drill.
4. Breaking ground ; tools employed ; blasting by vari-
ous methods ; machine drills ; driving leveb' and sinking
shafts."
5. Principles of employment of mining labour.
6. Means of securing excavations by timber or masonry.
7. Exploitation, or the working away of strata or veins,
8. Carriage or transport of minerals through under-
ground roads.
9. Winding, or raising- in the shafts, with the machinery
and apparatus required.
10. Drainage of mines, adit-levels, pumps, pumping^
engines. "^
it. Ventilation and lighting of mines.
12; Means of descending into and ascending from
mines.
13. IJressing or mechanical preparation of minerals.
14. Recent legislation affecting mines in the United
Kingdom.
15. Accidents in mines.
16. Useful minerals produced in various parts of the
globe.
1. Manner in which the Useful Minerals Occur. — The
repositories of the useful minera!s may be classified accord-
ing to their shape as (A) tabular deposits, and (B) masses.
A. Tabular Deposits. — These are deposits which have 8
more or less flattened or sheet-like form. They may be
divided, according to their origin, into (\) beds or strata,
and (2) mineral veins or lodes.
(1) Beds. — Geology teaches us that a large proportion stnrtia*
of the rocks met with at the surface of the earth consist deposit!.
of .substances arranged in distinct layers, owing to the fact
that these rocks have been formed at the bottom of seas,
lakes, or rivers by the gradual deposition of sediment, by
precipitation from solutions, and by the growth or accumu-
lation of animal and vegetable organisms. If any one of
these layers consists of a useful mineral, or contains enough
to make it valuable, we say that we have a deposit in the
form of a bed, stratum, or seam. Of course the most
important of all bedded or stratified deposits is coal, but,
in addition, wo have beds of anthracite, lignite, iron ore,
especially iu the Oolitic rocks, cupriferous shale, lead-
bearing sandstone, silver-bearing sandstone, diamond-,
gold-, and tin-bearing gravels, to say nothing of sulphur,
rock-salt, clays, various kinds of stone, such as limestone
and gypsum, oil-shale, alum-shalo, and slate.
The characteristic feature of a bed is that it is a member
of a series of stratified rocks ; the layer above it is called
the roof oi the deposit, and the one below it is the ^/ooa
Its thickness is the distance from the roof to the floor at
right angles to the plunes of stratification ; its dip is tho
I N I N G
441
inclination! downwards measured from tie horizontal; its
strike is the direction of a horizontal line drawn in the
middle plane.
The thickness of beds that are worked varies within
very wide limits. • Whilst the thickness of certain workable
beds of coal is only 1 foot, and that of the Mansfeld
cupriferous shale only 10 to 20 inches, we find on the
other hand one of the beds of lead-bearing sandstone at
Mechernich no less than 86 feet thick, and beds of slate
far exceeding that thickness. It- must not be supposed,
however, that the thickness of a bed necessarOy remains
uniform. Occasionally this is the case over a very large
area ; but frequently the thickness varies, and the bed may
dwindle away gradually, or in- ^
crease in size, or become divided
into two owing to the appearance
of a parting of valueless rock.
Fig. 1 shows beds of shale, lime-
stone, iron ore, and sandstone.
Any one of these beds may be
valuable enough to be worked. Fig. 1.
I (2) Mineral Veins or Lodes. — Veins or lodes are tabular
or sheet- like deposits of mineral which have been formed
since the rocks by which they are surrounded ; they differ,
therefore, by their subsequent origin from beds, which, as
jugt stated, are of contemporaneous origin with the enclos-
ing rocks (although of course cases occur in which the
deposit is lying uuconformably upon very much older
strata, or is covered uuconformably by very much younger
strata). It is necessary to explain that the term ".vein"
in this definition ii used in a more restricted sense than is
sometimes customary among miners, who speak of veins
of coal, clay-ironstone, and slate, which geologically are
true beds. They see a band of valuable mineral or rock,
and, careless of its origin, call it metaphorically a vein or
seam. On the other hand, the definition is broader than
that which prevails among some geologists, who would
confine the term vein to deposits occupying spaces formed
by fissures.
The term " lode " was defined itf 1877 by Mr Justice Field in the
celebrated Eureka ti. Richmond cx'ie as follows; — "We are ,of opinion,
therefore, that the term, as used in the Acts of Congress, is applic-
able to any zone or belt of mineralized rock lying within bound-
aries clearly separating it from the neighbouring rocks." This,
interpretation seems suitable for the peculiar mining tenure of the
TTnited States, where the discoverer of a vein or lode can obtain
a mining claim of 600 yards in length along the lode. It protects
the prospector, whose object is to obtain a secure title, the mode of
origin of the deposit being a matter of small importance to him so long
as it is worth working. In many cases also it would be impossible
to decide upon the mode of origin until workings had progressed
considerably, and even then there would be room for disputes.
No doubt a very large number of mineral veins are
simply the contents of fissures ; others are bands of rock
impregnated with ore adjacent to fissures or planes of
separation ; others, again, have been formed by the more
or less complete replacement of the constituents of the
original rock by particles of ore.
Veins may occur in igneous or in sedimentary rocks,
and in the latter they frequently cut across the planes of
stratification.
Like a bed, a vein has its dip and strike ; but, as the dip of veins
is generally great, the inclination is usually measured from the
vertical, and is then spoken of as the underlie or hade. The
bounding planes of a vein are called the walls or cheeks, and they
ere frequently smooth and striated, sho\ring that one side must have
•lid against the other. The upper wall is known as the Hanging
vail, the lower one as the fool wall. The width of a vein is
measured at right angles to the walls.
* A typical example of a fissure-vein is shown in fig. 2, repre-
senting a lead lode in slate at Wheal Mary Ann mine' in Cornwall.
' 0. Le Neve Foster, ' ' RemorlvS on the Lode at Wheal Mary Ann,
Menheniot," Tra-ns. Roy. Geol. Soc. Cornwall, vol. is. p. 153.
It is evident that a fisature in ths aniTounding sUte has here been
aued np by the successive deposition of banda of mineral on both
Slues.
A large proportion of the contents of a lode may consist of
fragments of the vi;alU that have faUen into the original fissure, and
these are often tightly cemented ■
together by minerals that have I
been introduced subsequently. TSe I
horizontal section of part of the i
Comstock lode- (Plate IV.) shows j
much "country" rock enclosed;
within the walls.
Where a lode consists of rock '•
impregnated with ore, the mineral-
iiiea part may fade away gradually
into the surrounding rock(aiu7i(ry)
without there being any distinct „ _
wall, as shown in tig. 3, which is an illustration" taken from the
(jreat i iat Lode-' near Redruth in Cornwall.
_ The celebrated Ruby Hill deposit in the Eureka district, Nevada
13 a mineralized zone of dolo- '
mitic limestone varying in
width from a few inches to .. -'■.)i,--b>;™j
4S0 feet, and having a mean "iV j)#^'«*«x
width of 250 feet. It con- <,.J>;'''
tains numerous irregular ore- ^ »- "* \
bodies, which consist mainly •>-*< >-,* '■y-v*-(i
of highly ferruginous car- ciiANtTr.
bonate of lead, rich in s,ilver
and gold. This mineralized
limestone band, long called Fig. 3.
a lode by miners, has been determined by the decision just men-
tioned to be a lode in the eyes of the law.
Yeins often continue for a great distance along their strike. The
Van lode in Montgomeryshii-e is known for a: length of 9 miles,
whilst the Great Quartz Vein in California has been traced for a
distance of no less than 80 miles. Veins are of less uniform pro-
ductiveness than beds, and are rarely worth working througliput.
Rich portions alternate with poor or worthless portions. The rich
parts have received various names according to the foi-ms they
assume : fi^. 4 represents a
longitudinal section along the ■
strike {coitrse) of a lode, and , ^-"'^ ''''^"'.y^.;----?^'^^^
the stippled parts are ore- ^ * ""
bodies; B, B,B are {wncAss; A '" .'Sfr
is a large bimch or course of
ore ; when an ore-body forms
a sort of continuous column
we have a sJioot, and ore-
bodies which on being ex-
cavated leave chimney-like
Fig. 4.
openings are called pipes (fitj. 4, C). In the United States the'
Spanish word toianza, literally meaning "fair weather" or "pro-
sperity," is frequently used for a rich body of ore.
The richness of veins is dependent in many cases upon the nature
of the adjacent rock (conntry), upon the underlie, and upon the
strike, variations in any one of these three elements being often
sufficient to cause a decided change of productiveness.
Various theories have been forraecf concerning the origin of
mineral veins. Some geologists suppose that the minerula now
constituting the veins have been dissolved out of the adjacent rocks
and re-deposited in the vein cavity ; others, on the contrary, believe
that the ores have been brought up from great depths by mineral
springs. In all probability both theories are correct, some lodes
having been formed by the former process and some by the latter ;
and, furthermore, other lodes appear to owe their origin to a gradual
substitution of valuable minerals in the place of some of the con-
stituents of a worthless rock. One of the most important con-
tributions to the science of ore-deposits of late years has been
the discovery by Professor F. Sandberger of small quantities of
silver, lead, copper, nickel, cobalt, bismuth, arsenic, antimony,
and tin'in silicates, such as olivine, angite, hornblende, and mica,
which are constituents of igneous rocks. He therefore regards
these rocks as the sources from which lodes have derived their
riches.
B. Masses. — These are deposits of mineral, often of Mosses,
irregular shapes, which cannot be distinctly recognized as
beds or veins. Such, for instance, are the red hematite
' James D. Hague, in United Slates Geological Exploration of the
Fortieth Parallel, vol. iii., "Minliig Industry," Washington, 1870,
Atlas, plate 11.
3 C. Le Neve Foster, "On the Great Flat Lode south of Red>
ruth and Camborne, and on some other Tin Deposits formed by
the Alteration of Granite," Quart. Jour. Oeol. Soc, vol. ixiiv. p.
644.
]i;— 17^
442
MINING
[PKOSPBOTINO,-
deposits of (.he TJlveraton district (fig. 5') and the brown
hsematite deposits {chums), of the Forest of Dean, which
f\Q. 6.--Vertical Section, Roauhead Mid« A, Moontain Limestone ;
B, red hematite , C, sand and clay, D, gravel Seals ^^i^.
occupy irregular cavities in the Mountain Limestone. These
may have been formed by the percolation of water bring-
ing dovm iron in solution . from overlying Triassic rocks.
Other examples of masses
are the calamine deposits of
Altenberg^ (fig. 6), Sardinia,
and Lombardy, the iron ore </af^.\ll|)|||l''f=^---\l; lig;:!^^
deposits in Missouri, such ^^^fl | Wii=5J|j§^^^^
as Iron Mountain and Pilot ^^iJ^^!ll||'j|)^^^|l||^^^^
Knob the huge upright j,„ e.-VertlcJi^tionl Allen-
necks or " pipes of dia- bei-g. B, elate ; d, dolomite ;
mantiferous rock in South C, calamine ; L, clay.
Africa, and the granite decomposed in situ worked for
china clay in CoruwaU.
Under this head also are included by most authors the
so-called " stockworks " or " reticulated masses," names
applied to masses of sedimentary or igneous rock which
are penetrated by so many little mineral veins as to make
the whole worth excavating.
It must be understood that we ca'lmet e3r.«ct nature to make
distinct lines of demarcation between the different kinds of
deposits. Though we may be able to see clearly that a seam ot
coal is contemporaneous with the enclosing rocks, and that a vein
intersecting beds of shale and sandstone was formed subsequently,
cases frequently occur where the origin of the mineral is uncertain.
For example, we have the lead-bearing sandstone ofMechernidiand
the silver-bearing sandstone of Utah. The grains of sand are of
sedimentary origin ; but opinions differ as to whether the lead and "
silver respectively were deposited with the sand or were introduced
subsequently by solutions percolating through the beds. In the
case of the well-known bed of Cleveland ironstone, Dr Sorby
considers that the iron was "derived partly from mechanical
deposition and partly from subsequent chemical replacement of
the originally deposited carbonate of lime." ^ Furthermore, a bed
may be so folded and.contracted as to lose itj original sheet-like
form in places and assume the shape of au irregular mass. This
may happen even with a coal seam.^
AU kinds of deposits are subject not only to irregularities of
origin dependent upon their mode of formation but also to dislo-
cations or shiftings known as faults, heaves, or throws.
We iviU take the case of a bed (fig. 7). AB is a seam which ends
off suddenly at B, whilst the continuation is found at a lower level
St CD. The bed was evidently once continuous ; but a fracture took
place along the line XY foUowetl by a displacement. As a rule
Fig. 7. Fig. 8.
the portion of rock on the hanging-wall side of a fault appears to
have slid downwards, but occasionally this is not so, and wo have a
reversed fault (fig. 8). It is very evident, in some cases, that the
motion took place, not along the line of greatest dip, but in a dia-
* Ft^ Moritz WolfT, " Beschreibung der Rotheisenerzlagerstattoa
von West Cumberland und North Lancashire," Slahl und £isen, 2
•Tahrgang, No. 12, plate vL
^ * M. Braun, Zcitscfi/r. d. d. geol. Oesdhch.y 1857, vol. ix. ; and A.
7on Groddeck, Dit Lehre von den LagersUUten der Erie, Leipsic,
1879, p. 232.
' Qitart, Jour. Oeol. JSoc, vol. xxzv, (1879), p. 85, Anniversary
Address of the President.
' J. Callon, Lectures on Mining, vol. i. p. 03, and Atlas, plate
viii. fig. 44.
gonal direction, causing a displacement sideways as well as down-
wards. Nevertheless, where beds or veins are not horizontal, a men
shift along the line of dip is sufficient to cause an apparent heave
Let AB and CD
sideways. This will be understood from
represent two portions of a lode dislo-
cated by the fault EF. The point B'
corresponded originally with B, and
the dislocation was caused by a simple
eliding of B' along the line of dip BB'.
An instance of the complication caused
by a succession of faults is shown in
fig. 10. »
2. Prospecting^ or Search for
Mineral.-rThe object cf the pro
spector is to discover valuable rteposits of mineral. This
search is beset with many difficulties : the outcrops of
ProsptA
Fia. 10.— Vertical Section, PenhaUa Mine, Cornwall. G, G, G, small
veins called gossans in the St Agnes district.
mineral deposits are frequently hidden by soil; the nature
of the deposit itself is generally entirely changed near ibt
surface; and, in addition to this, the explore.' may have
to pursue his work in trackless forests far away from any
settlements.
The prospector seeks for natural sections of the rocks,
such . as occur in cliffs or in river valleys and their tributary
gullies and gorges ; he examines the materials constituting
the river-beds, often digging up and washing portions in a
pan, in order to ascertain whether they contain traces of
the heavy ores or metals. If, while prospecting in a valley,
ho discovers stones that have the appearance of having onca
belonged to veins, he endeavours to trace them to their
source, and is perhaps rewarded by finding similar frag-
ments, but less water-worn, as he goes up the stream ;
further on he may come upon large blocks of veinstufE
lying about, and -finally find the vein itself laid bare in a
gorge, or at the bottom of a brook, or possibly projecting
above the sod in the form of huge crags of quartz. Thus
at the Great Western quicksilver mine in California the
outcrop of the vein appears as a dike over 100 feet wide,
and having precipitous sides in places'75 feet'high.^ Loose
pieces of veinstuff found lying about are known in
Cornwall as shoad-stonos, and shoading is the term given
to the process of tracking them to the parent lode.
The upper portion of a deposit is frequently much altered by
atmospheric agencies, and bears little resemblance to tho undecom-
posed bed or vein which will eventually be mot with at a greater
or lessor depth. The principal difference consists in tho change of
sulphides into ojddes or oxidised compounds. Thus iron pyrites,
which is such a common constituent of mineral veins, is converted
into hydratcd oxide of iron, and a vein originally consisting largely
of iron pyrites and quartz now becomes a cindcry mixture of cjuartat
and ocliro, known in Cornwall as gossan. This gossan, of iro»
hat, may often furnish important indications concerning the natura
of tho lode itself, because such minerals as pyromorphito or ccrus-
site point to the existence of galena, whilst melaconite, cuprite,
malachite, and azurita are th« forerunners of chalcopj-rite or copper
glance. The gossan itself may contain a suflicient quantity of valu-
able ores to be worth working.
The seams containing native sulphur in Sicily often show no trace
of that clement immediately at the surface, as the 8ujphur-be.ar-
ing liincstono weathers into a soft white granular or pulverulent
' J. W. Pike, " On some remarkable hea\fs or UrouK in PenhaUs
Mine," Quart. Jour. Qcot. Soc. , vol. xxii. p. 537.
' Luther Wagoner, " Tho Geology of tho Quicksilver Jlinos of Cali-
fornia," Engineering and Jfiiiit.j Journal, vol. ucxiv. p. 334.
BOUXNO.]
MINING
443
Saring.
Boring
Trith
rods.
variety of gypsum, called hriscaU by the miners, and considered
by tbem as aifording important indications concerning the bed
itsell^
I Other signs of mineral deposits are given by springs and by
certain plants dependent upon the depofiit or its associated minerals
for part of their nourishment. The appearance of the so-caUed
lode-lights may be explained by the production of phosphoretted
hydrogen from the action of organic matter and water upon phos-
phates, which are so common in the upper parts of mineral veins;
and one hears also of differences in the appearance of the vegetation
along the line of the deposit, of places where snow will not lie in
winter, and of vapours hanging over the ground. Though some
writers refuse to put any value upon these indications, they should
not be entirely overlooked, because the outcrop of a lode, of different
nature and texture to the surrounding rock.% and which is generally
a channel for water, may readily cause the phenomena just men-
tioned. Where the surface is cultivated and the natural springs
are tapped by adit-levels or other mine-workings, these appearances
cannot be looked for to any great extent. "With one special
mineral, magnetic iron, the position of the deposit may be traced
out with some degree of accuracy with a dipping needle ; this is
used in Sweden.
After having acquired an idea of the position of a vein
or seam by some of the surface indications just mentioned,
it is necessary, before attacking it by shafts or levels, to
obtain more certain data concerning it. In the case of
mineral veins, trenches are dug at right angles to the
supposed strike; and, when the upper part of the deposit
has been cut in several places, its general course and dip
can be determined sufficiently for the purpose of arranging
the future workings. These trenches are called " costean
pits"; in some eases, instead of a trench, a pit is sunk a
short distance and a little tunnel driven out.
Where the mineral to be wrought occurs as a bed or
mass, the process of boring is resorted to, and indeed this
method is also applied in the case of veins, especially in
the United States. Boring is a work of such importance
'.hat it deserves to be treated under a separate heading.
3. Boring with Rods and Ropes — Diamond Drills. — The
object of boring is to reach a deposit by a small hole and
a.scertain its nature, its depth from the surface, thickness,
dip, and strike. Bore-holes are also used for obtaining
water, brine, and petroleum, which either rise to the
surface or have to be pumped up from a certain depth, and
finally for tapping water in old workings or for effecting
ventilation. The methods of boring may be classified as
follows: — (1) boring with the rod; (2) boring with the
rope ; (3) boring with the diamond drilL
In the first method tools for cutting and removing the
rock are fixed to rods, which are lengthened as the hole
increases in depth, and which are worked by hand or by
machinery at the surface. Where the ground is soft, such
as sand or clay, tools like augers can be employed ; but in
harder ground it becomes necessary to have recourse to
percussion ; various forms of chisel are used, the simplest
being made of the shape shov.-n in fig. 11.^ The rods
generally consist of bars of square
iron, from 1 inch to 2 inches on the
side. The length of each rod de-
pends upon the height of the tower,
derrick, or shears erected above the
bore-hole, which should be an exact
multiple of the individual parts.
These are made in lengths of 15 to
30 or rarely 40 feet, and with a
suitable tower it is possible to de- ^"^ "-ChiseU. Fig. 12.
tach or attach two or three lengths at a time, instead of
having to make or unmake every joint. The mode of con-
nexion usually preferred is by a screw joint as shown in
fig. 12 ; care is taken to have all the joints exactly alike,
so that any two bars can be screwed together. In order to
&
■ ' torcnzo Parodi, Suit EUrtaifiru dello Sol/o in Sicilia, 1873,
yp. 7 and 24.
• Serlo, Lcitfadc.i zur Scrgtautunde, Berlm, 1876, p. o9.
diminish the weight of the rods, which becomes consider
able in deep holes, wood has sometimes been employed.
The rods are connected by male and female screws attached
to the rods by sockets of sheet iron, or by a fork-like
arrangement. At the surface a head is screwed to the
uppermost rod by which the rods can be lifted, and they
are turned by means of cross-bars called tillers.
When the depth is small the rods are lifted by hand and then
allowed to drop, being turned slightly at each lift so that the
cutting chisel may strike a new place each time. For greater
depths a lever has to be employed, the rods being suspended at one
end, whilst the other end can be pressed down by men using their
hands or feet. The spring pole is another arrangement, in which
the elasticity of a long pole is made use of for lifting the rod at each
stroke. The length of the stroke can be maintained the same while
the bore-hole is deepened by means of a screw in a swivel-head at
the top of the rod.
With deep holes, and especially those of large diameter, steam
machinery has to be employed for working the rod ; the engine
may be direct-acting and stand immediately above the bore-hole,
but a commoner arrangement is to employ a single-acting cylinder
working a beam. Occasionally also the beam is actuated by a
connecting-rod worked by a crank.
The actual boring machinery has now been described, and the
mere boring appears to be a very simple matter, consisting only in
lifting the roa a little and allowing it to drop, the rod being turned
slightly before each stroke. Nevertheless the process of putting
down a bore-hole is not so simple as it seems, for there are numer-
ous indispensable accessory operations which take up much time«
In the first place the debris have to be removed, and in order to
effect this the rods must be drawn up, the swivel-head is discon-
nected and a cap screwed on. , A length of rods is now drawn up by
a hand or steam windlass and disconnected. It is well to have as
many caps as there are lengths to be drawn up, and then each length
can be suspended in the house. Sometimes a grip which catches the
rod at the bulging joint is used instead of a cap. The next operation
consists in lowering by means of a rope the shell-pump or
sludger, which is a hollow cylinder with a clack or a ball-
valve (fig. 13). It is worked up and down a little till it is
filled, and it is then drawn up and emptied at the surface.
The operation ii repeated, if necessary, and the boring is
resumed with the rod.
Occasionally a bore-hole has to be widened slightly with
a tool called a reamer. Soft beds may have to be bored
through with a unmble ; and, unless the rocks are hard and
firm, the hole has to be lined with a tube, generally of sheet-
iron. Accidents may occur, causing an immense amount '^K* y''
of trouble, such as the breaking of rods or chisel, and many in-
genious implements have been devised for seizing the broken rod
or the fragments, of tools which prevent further progress
with the work.
In boring at considerable depths, the weight of the
rod becomes so great that much vibration ensues when
the mass is suddenly arrested by the chisel striking
against the bottom of the hole. VarioBS devices have
been conti-ived for overcoming this difficulty and pro-
ducing a tool which will act independently of the rod.
One of the best-known arrangements is the free-falling
tool invented by Kind (fig, 14).' The head of the actual
boring-rod is held by a click or grapple ; when the main
rod descends, the resistance of the water in the hole
slightly stoi>3 the sliding disk D, the jaws J, J open, the
head is disengaged, and the boring part falls and strikes
the bottom without any injurious vibrations being com-
municated to the main rod. When this descends farther
the head is caught again by the click. Special tools also
are used for cutting an annular groove at the bottom of
a borehole and breaking off the core, which is then
brought up, with certain precautions, so as to show the
nature and dip of the strata traversed.
In order to obviate the great loss of time which Q %f^
ensues from connecting and disconnecting long
lengths of rods, recourse may be had to boring
with the rope. In this method, known as the
Chinese method, the chisel is worked by a rope in *«• •
the same manner as the sludger already described. Messrs
Mather and Piatt of Manchester have long used with suc-
cess, in many parts of England and various other countnes,
a system of boring by means of a flat hempen rope.
The most important modification of late year? m tb<»
» J. Gallon, Lectures m Mining, voL L, Atlas, plat^j ix. fig. £2.
444
MINING
[BfiEAKiNO OnOUKD.
ili
iiTi-^"
Fio. 16.— Diamond
DrUl,
tWnni'n'l procoHs of makinf; horo )\oloB ifl the inti'oduction of llio
*•''"• diamond drill. Tlio working part of tUo drill eoniiiiita of
Iho BO-<:allod crown, which is a Hhort pioco of tuLo nmdo of
cast ijtool, at ono end of which o, number of black diamonds
are foBtuncd into small cavitioa (lig. 15).
Tho crown in Horowed on to wrought-
iron pipoB, which constituto tho boring
rod. Machinery at the surface camiiv)
tho rod to rotate, and tho result is tho
cutting of an annular groove at the
bottom of tho hole, leaving a core,
which, brcmking off from time to time,
is caught by a little shoulder, and
brought up to tho surface with tho rod. ' \
In places where it is not necessary to V
make any verification of tho rocks tra-
versed, the crown is arranged with
diamonds in tho centre also. The
diSbris, in either ca.se, are washed away by a stream of
■water, which is forced down the tube and flows up tho sides
of tho hole. With this system a bore-hole can bo deepened
continuously at a speed altogether unattainable by tho
other methods, which require stoppages for cleaning out.
It has the further advantage of making it possible to drill
holes in any direction ; and prospecting diamond drills are
constantly used with much success inside many metal mines,
especially in tho United States.
Fig. 10^ shows the Littlo Cham])ion Rock-Drill, which is largely em-
ployed in tlio Lake Superior district for prospecting. It can bo used
above or bolo'w gi-ound. Two inclined cylinders arivo a horizontal
crank shaft, which works bevel gear, causing the drill to revolve. At
the same time a countershaft is likewise set in motion, and this effects
tho advance of tho drill by gearing driving the feed-screw; as there
are throe kinds of gearing, the si>eed can be varied at pleasure. Tho
feed -screw and its connexions are cai'ried by a swivel-head, and this
can be turned so as to drill holes at an angle. The drum shown
above the cylinders is used for hoisting out trie drill-rods by a rope.
Tho rods aro lap- welded iron tubes 1 { mchcs in diameter, fitted with
a bayonet joint.
Another light portable prospecting drill for underground work is
Fio. 16.— Littlo ClKimpi
tk-Drill. Fig. 17.
represented in fig. 17.' It is intended for drilling holes 1} inches
in diameter to a depth of 150 feet. The cores which it yields are
5 inch in diameter. It has double oscillating cylinders 35 inches in
diameter with 34 inches stroke, which are run up to a speed of 800
revolutions. The drill can bo sot to bore in any direction by
turning the swivel-head on which it is carried.
The larger rock-drill used by tho American Diamond Rock
Boring Company for putting down holes to a depth of 2000 foot
consists of a 20 hoi-sc-powor boiler with two oscillating 6-iuch
cylinders and tho necessary gearing for working the drill, all
* Enginecnng and Mining Jqut.^ vol. xxiiii. p. 110.
' Ibid., vol xixin. D. 273.
mounted upon a carriage, iic tJiat tho whole raachiuo is readily
moved from place to place. The feed iu cfTected by gearing or by
hydraulic pieesuroj a 28-inch crown is employed, leaving a 2-iuch
core. Each soparato drill'rod is 10 feet long. The total weight of
the machine is about 4 tons.
4. JireaHiuj Ground — Tools Employed — Blasting by
Various Melliodji — Alrrrhine Drills — Driving Levds and
Sinking Shaft). — ITie kind of ground in which mjning ex-
cavations have to be carried on varies within tho widest
limits, from loose quick.sands to rocks which are eo hard
that tho best steel tools will scarcely touch them.
Loose ground can bo removed with tho Ehovel ; but in TooU
the special case of peat sharp spudos are employed, which
"i l-ho fibres and furnit^h lumps or sods of con-
.■■; for drying and subsequent use as fuel. What
/.(!>, soft, or easy ground, such as clay, shale,
(lecouipoocd clay-slate,
and chalk, requires
tho use of the pick
and the shovel. The
pick is a tool of very
variable form, accord-
ing to the material
operated on. Thus
there aro the navvy's
pii-'i, tho single-point-
ed jiick with a striking
head at the other end called the poll-
pick (fig. 18), and numerous varieties
of the double-pointed pick (fig. 19), tho
special tool of the collier, but aico
largely used in metal mining. When
the ground, though harder, is neverthe-
less "jointy," or traversed by many
natural fissures, the wedge comes into no. 1!>.— Donble-
play. The Cornish tool known as a gad pointed Pick.
is a pointed wedge (fig. 20). The so-called "pick and
gad " work consists in breaking away the easy ground with
tho point of tho pick, wedging off pieces with tho gad driven
iu by a sledge or tho poll of tho pick, or prizing them
off with the pick after they have been loosened by
the gad. The Saxon gad is held on a little handle, i
and is struck with a hammer. It is used for wodg
ing off pieces of jointy ground, and in former days \
even hard rocks were e.xcavatod by its aid. The
process consisted in chipping out a scries of parallel ^q,"?'
grooves and then chipping away tho ridges left
between the grooves. As a method of v. orking this process
is obsolete; but' it is useful on a small scale for cutting
recesses (hitches) for timber, for dressing tho sides of levels
or shafts before putting in dams, and for doing work
in places whore blasting might injure pumps or
other machinery.
We now come to hard ground ; and in this class
we have a large proportion of the rocks met with
by the miner, such as slate of various kinds, hard
grits aud sandstone, limestone, the metamorphic
schists, granite, and the contents of many mineral
veins. Kocks of this kind are attacked by boring
and blasting. The tools employed are the jumper,
the borer or drill, the hammer, the sledge (mallet,
Cornwall), tho scraper and charger, tho tamping bar
or stommer, in .some places the pricker or noodle,
'he claying bar, the crowlmr, and finally the shovel
i^r clearing away the broken rock.
The jumper (fig. 21) is merely a long bar of iron
terminating in two chisel-like edges made of steel; Fig. 21.
generally there is a swelling in the middle, and
sometimes the jumper tapers all the way from the middle
to the edge or bit. The jumper is most commonly used
when it is necessary to bore holes downwards, and is
tAPLOSIVES.]
MINING
445
Eipio
sires.
largely employed iq quarries; occasionally it is used m
boring holes horizontally, as for instance in the salt mines of
Cheshire. The jumper is held in the desired direc-
tion, lifted up, and thrust down; it is tuned a
little after each stroke.
However, the miner's tool is generally the borer
proper, or drill (fig. 22), which is a bar of round or
octagonal steel, usually from | inch to 1 J inches in
diameter, with one end forged i^to a chisel-shaped
edge, the exact shape and degree of sharpness
varying according to the hardness of the rock.
The hole is bored by striking the drill with a
hammer or sledge and turning it after each blow.
Boring is said to bo single-handed if the miner
holds the dtill iu one hand and strikes with the hammer
in the other, whilst it is called double-handed -.vhen one
man turns and an-
other strikes. The
hammers for single-
handed boring usu-
ally vary in weight ©
from 2 to 6 or 7 ft. F'o. 23.— Sledgo-Hammer.
The double-handed boring hammer, or sledge (fig. 23),
weighs from 6 to 10 lb or more. If a hole is directed
downwards, the miner pours in a little water and bores the
hole wet. From time to time he draws out the sludge with
the scraper, a little disk at the end of a metal rod, and he
takes a fresh borer when the tool he is using has become
blunt. The depth bored varies with the rock and the nature
of the excavation ; but in driving levels in the ordinary
way the depth is commonly from 18 inches to 3 feet.
' Holes for blasting are sometimes bored by tools like
carpenters' augers. One of the simplest, which is used in
some French slate-mines, is very like a brace and bit, and
the tool is kept pressed against the rock by means of a
screw fixsd in a frame resting on the ground.
The pricker, or needle, is a slender tapering rod of copper
or bronze, with a ring at the large end. It is used lor
maintaining a hole in the tamping through which the
charge can be fired. The use of needles made of iron is
prohibited in many countries, on account of the danger of
their striking sparks which might fire the charge. The
tamping bar, or stemmer, is a rod of iron, copper, or bronze,
or iron shod with copper, and it is used for ramming in
dried clay, slate pounded up, or other fine material, upon
the powder, and so creating a resistance sufficient to make
the gases generated by the explosion of the charge rend
the rock in the manner required. The claying bar is used
for lining wet holes with clay, and so rendering them
temporarily watertight.
Shovels vary much in different districts. In the south-
west of England the long-handled shovel is preferred to the
common one with a short handle ; in Germany the ore or
rubbish is frequently scraped into a tray with a sort of hoe.
In addition to those tools the miner requires an ex-
plosive, and a means of firing the charge at the bottom
of the hole which will give him time to escape. Twenty
years ago gunpowder was the only explosive in common use
in mines, but at the present day its place has been taken to
a very large extent by mixtures containing nitroglycerin or
gun-cotton. The powder used for blasting in mines usually
contains less saltpetre than that which is employed for
sporting or military purposes. The following is an analysis
of mining powder by Captain Noble and Sir F. Abel:'-
Saltpetre
..61 66
.. 012
.. 014
.. 16-06
.. 17 '93
.. 0-66
2'23
Potassium sulphate...
0-59
,, chloriJo...
Water
1-61
Carbon
Hydrogen
" "On Fired Gunpowder," Phil. Trant., 1880, p. 225.
Gunpowder compressed into cylinders of diameters
suitable for bore-holes, and provided with a central hole
for the insertion of the fuse, has lately beeii brought
forward with some success.
Nitro-glycerin or glyceryl nitrate is a light-yellow oily
liquid which is very sensitive to shocks ; under the action
of a fulminating cap it explodes with great violence.
Its chemical composition is expressed by the formula
C3Hi(N02)303 or (CjHJSNO,; its specific gravity ia
V6. It has been found so dangerous that its use by
itself has been given up ; but on the other hand the mix-
ture of nitro-glycerin and infusorial earth (Zsese^^uA?-) called
dynamite or giant powder is now one of the commonest
explosives met with. It has the advantage over powder
that it is far more powerful, that it may be used in wet
holes or under water, that it is very effective even in
ground full of " vughs" or cavities, and that it requires no
hard tamping, which is always a source of danger. Its
plasticity too enables it to fill the space at the bottom of a
bore-holo, which is rarely a true cylinder, more completely
than any solid cartridge can do. One disadvantage is
that it has to be thawed in cold weather, and there is also
the fact that occasionally the whole of a charge of dyna-
mite fails to go off, and unnoticed remnants have exploded
and caused serious and even fatal accidents when struck
with the pick or borer. The danger is enhanced when tha
remnants have been left in contact with water, which causes
a separation of the sensitive nitro-glycerin, so that even' a
blow upon the adjacent rock may lead to an accident if
any of the explosive oil has leaked into cracks. The
strongest dynamite coitains about 75 per cent, of nitro-
glycerin, the rest being kieselguhr. A newer explosive is
blasting gelatin; it is made by mixing nitro-cotton with
nitro-glycerin, until enough nitro-cotton has been dissolved
to convert the nitro-glycerin into a jelly-like mass. The
blasting gelatin in ordinary use contains no less than 93
per cent, of nitro-glycerin, with 7 per cent, of nitro-cotton,
and its strength is very great.
Gun-cotton per se is not much in favour in ordinary
mining; but mixed with some nitrate or mixture of
nitrates, such as the nitrates of barium and potassium, and
known as cotton powder, tonite, and potentite, it is
employed extensively. Though not quite so powerful as
dynamite, nitrated gun-cotton possesses the important
advantage of not requiring to be thawed in cold weather.
As in the case of dynamite, accidents have been caused by
remnants of charges ; and with both explosives it is neces-
sary to examine carefully the bottoms of all holes after
blasting, and to destroy any possible remnants by firing off
a detonator in any bottom or " socket" which cannot with
certainty be pronounced free from danger.
The commonest method of firing a charge is by means SafotjH
of the safety-fuse, a cord containing a core of gunpowder '"""•
introduced during the process of manufacture ; it may be
rendered waterproof by tar or gutta-percha.
In blasting in the ordinary way the charge of gunpowder is put
in either loose or enclosed in a paper bag, and it is pressed down to
the bottom of the hole with a wooden stick, whilst a piece of fuse
also is inserted extending from the charge well beyond the hole.
If the powder is loose the miner carefully wipes down the sides of
tlio hole with a. wet swab stick (a wooden rod witli the fibres frayed
at one end), or with a wisp of hay twisted round the scraper, in
order to remove any loose grains adhering to the fuse or the sidea
of the hole, and then presses in a wad of hay or paper. A littlo
fine tamping, often the dust from borinff a dry hole, is now thrown
in ^nd rammed down with the wooden charging stick, and the same
process ia repeated, and when harder tamping is required the metal
bar ia brought into operation, until the hole is completely filled.
As the safety fuse burns slowly, at the rate of about 2 or 3 feet
a minute, the miner can secure ample time tUt retreat by taking a,
sufficient length. It is usual to iguito the fuse by a candle-end
fixed under it by a piece of clay, and it takes a little time for tha
candlo to buj-n through the fuse,
Tha old plan of firine a charge, which is still in use in many
446
MINING
[blastdjo.
places, consists in inserting the needle into the charge and then
tamping up the hole. Care is taken to draw out the needle a little
as the tamping proceeds, so'as to prevent too much force being re-
quired for its final withdrawal. The small hole left in this way
serves for the insertion of a straw, rush, or series of small quills, filled
with fine powder, which like the fuse reaches from the charge to
the outside. A short squib which shoots a stream of sparks down
the needle hole is al-.o used occasionally. Tlie straw or squib is
lighted by some kind of slow match, made either by dipping a
cotton strand in melted sulphur or soaking a piece of paper or a
lucifer in the tallow of a candle ; touch-paper also is used.
Dynamite, blasting gelatin, gun-cotton, and cotton-powder are
fired by the detonation of a fulminating cap. A long copper cap
containing fulminate of mercury is fastened into the safety-fuse by
Bqueezing with a pair of nippers, and is then inserted into a small
cartridge of the explosive (primer), and placed above the rest of the
charge. Fig. 24 shows a hole charger"
vith two dynamite cartridges, a primei
with cap, and filled up with water as
tamping. Sometimes gun-cotton is fired
by a small charge of powder above it.
Several substitutes for explosives
liave been tried mth the object of
cetting rid of the flame, which is
dangerous in collieries giving off fire-
damp. Among these may be men- // ^^^ \
tioned plugs of dry wood which swell /- /' "N^ >
■when wetted, wedges worked by/--
liydraulic pressure, cartridges con- Fig. 24
taining compressed air at e.'ctreraely
high pressures, and lastly cartridges of compressed lime which ex-
ftauds when water is brought into it.
For tlie purpose of firing several holes simultaneously,
Messrs Bickford, Smith, & Co., the original inventors and
makers of the. safety-fuse, have brought out a new fuse
(fig. 25), the action of which
will be easily understood
from the figure. An ordi-
nary fuse is fi.xed into a
metal case called the igniter,
from which a number of
instantaneous fuses convey fiie to as many separate holes.
It is found in practice that this fuse answers very well. •
Blactmg Charges may be readily fired singly or simultaneously
by eiw with the aid of electricity, cithei of high tension obtained
tr.city. fj.(,jjj a frictional, magneto-electric, or dynamo-electric
machiiie, or of low tension from a galvanic battery. The
former is preferred.
Fig. 26 shows a section of one of Braiu s high-tetfsion fiises.
A i'i .1 nylinMninl wonj.t, . ;isc containing a papei cArtridge 13,
Fig. 2S.
■with an eiectric igiiiting composition C at the bottom. Two
copper wir6s D, D enclosed in gutta percha E, E reach down to
the composition, where they are about -^ inch apart. A copper
cap or detonator G is fixed on to the small end of the wooden case.
The insulated wires D, D are long enough to reach beyond the bore*.
hole. The ends of the wires are scraped bare, and one wire of the
first hole is twisted together with a wire of the next hole, and so
on, and finally the two odd wires of the first and last hole are
connected to the two wires of a single cable, or to two separate
cables, extending to some place of safety to which the men can
retreat. Here the two cablo wires arc connected by binding screws
to a frictional electrical machine or dynamo exploder. A few turns
of the handle charge a condenser, and by pressing a knob or by
some other device the circuit is completed and tho discharge
effected. Tlic clectncity passes through tho fuse wires making a
spark at each break, and so firing tho electric igniting composition.
The flame flashes through the hole H, and ignites the fulminating
mercury I, the detonation of which causes the cxplo.^ion of tho
dynamite, blasting gelatin, or tonite surrounding the cap.
Otie great advantage of electric firing is that tho miner
can retire to a perfectly safe place before attefnpting to
explode the charge. This is important in sinking shafts,
where the means of escape are less easy than in levels.
A second advantage is that there is no danger of a " hang
fire," an occasional source of acciaents with the ordinary
safety-fuse.
One of the greatest improvements in the art of mining srechia-
during the last few years has been the introduction of thills,
machinery for boring holes for blasting ; most of the
machines imitate percu.s.sive boring by hand, but a few
rotary machines are also in use. A percussive drill oi
perforator consists of a cylinder with a piston to which
the drill is fastened. Compressed air is made to act
alternately on each side of the piston, and in this manner
the drill receives its reciprocating motion. Various
arrangements have been adopted for securing the automatic
rotation of the drill. In some cases also the advance
forward of the machine, as the hole is deepened, is also
effected automatically ; but in many of the best drills this
work is left to the man in charge. It is impossible within
the lim^^ "4 this article to describe the various drills now
in use, ci even to make a complete enumeration of them.
The following, iii alphabetical order, are the names of some of
the best-known drills t — Barrow, Beaumont, Burleigh, Champion,
Cornish, Cranston, Darlington, Desideratum, Dccring, Duboia
and Fi-anjois, Dynamic, Eclipse, Excelsior, Ferroux, Frohlich, Inger-
Eoll, Laxey, Mackean, Osterkampf, Kand, Roanhead, Sandycroft,
Schram. An account of two of the simplest, the Barrow and the
Darlington drills, will be sufliclent to give a general idea of the
construction of these machines.
" TThe Barrow drill (fig. 27) consists essentially of a gun-metal Barrow
o* drill.
14JJ
Fig. 27.
cylinder C about 2 feet in length and i inches in diameter, to
which works a cast-steel piston-rod D, fitted with two pistons G,
about 12 inches apart, mid-way between which is the tappet, or
boss, G'. In a valve-box on the top of the cylinder is placed the
oscillating slide-valve H (sho^vn separately), hinged at M, which
is worked by the reciprocation of the tappet G coming in con-
tact with its lower edges, which for this purpose are formed with
two slopes at each end, as shown. It has ports corresponding
with openings in the slide-valve face for admitting the fresn
steam or compressed air from tho inlet pipe I (fig. 28) to the
ports j at each end of tho cylinder, and for letting tiio spent o>
exhaust air or steam escape by the exhaust pipe J. This simple
arran"cnient constitutes the wliolo valve gear of the machine.
"tIio borer is inserted into a hole formed in tho fore cml of the
piston rod, and is fixed therein by means of a screw. Its rotation
13 efi'ccted by band, by means of the handle D", turning a spindlo
D', which is so fitted by means of the cotter d, made fast in tho
piston DG, and fitting in a slot in tho spindle D', that tho latti*
can slide in tho piston DO, but when turned by the handle causes
the piston to turn with it. The spimllo D' has a pinion E gearing
into tho pinion F, on tho adjusting and feeding; screw C, so that
wlien the piston D is turned by means of tlie handlo D" the
cylinder C is simulUncously pushed along tho bcd-plato A. 1^"^
pinions can bo easily disconnected by loosening the nut/, and thus
the piston and the adjusting screw can be turned independently of
one another when required. .
" Tho borers used are respectively 1 i inches, IJ inches, and 1 incti
in diameter, tho length of the stroke 4 inches, and the roaiimnm
number of blows about three hundred per minute Tlio air is
IIAOHCTB DRILLS.]
M I K I N (r
447
liooght down about 400 fethotos from erufico, at a preastue of £0 to
£6 lb to the sqnare mch, in wrought- iron pipoe 2 inehea in diameter in
the shaft, and lA fechea in the lerel, and aomitted through a flexible
tube into the inlet I on the left-hand side of the cylinder. The cost
of the pipes is rather npder Ti. a foot, or about Ss. 3d. per &thom.
The air is compressed* at the surface by a 14- inch compressor, worked
by a 12-inch horizontal engine, capable, however, of working two
E^^
machine drills. The gross weight of the machine, including tea
bed-plate and gudgeon, is about 116 lb."
Tne method of nxing the machine forworK 13 as foiiows : — '* The
bed-plate A of the machine is formed with a gudgeon A' which fits
into, and can be adjusted to any position in, a socket formed in or
on a clamp B',. which can be &xea on any part of the wrought- iron
bar or column B, thus forming a universal joint. This bar or column
Scale, figs. 29, 30.
lochn U 9 6 3 0 1 'i Feet.
Fio. 29.— Side Elevation of Darlington's Rock-DriU.— Scale I'jjV-
can be placed in position either horizontally or vertically, as may I adjusting screw M, and claws N and N'. If necessary, wooaen
be most convenient, but is generally placed across the level, against I wedges 0, 0' are diiven in between the claws and the vjall to make
the sides of which it is secured by means of the clamp L, and I it still firmer. The weight of the bar is about 120 ft."'
<x>
Fio. 30.— Horizontal Section of Darlington's Rock-Drill.— Scale ■^.
Air-compressing plant of greater size has now been erected at
Dolcoath mine, to which the above description refers. At Snail-
beach mine in Shropshire they have two air-compressors of 18 inches
Pig. 81.
diameter and 5 feet stroke ; the air-main is at first 9 inches iu dia-
meter, then 6 inches, whilst 2-mch ^-pipe is used in the levels.
A rock-driU which has done, and is doing, excellent work is that
of llr John Darlington. Its constraction will be xmderstood bv l^arUng-
reforring to figs. 29, 30, and 31 ; a is the cylinder, h the piston rod, ton drili
c the borer; rf, d are two openings for bringing in compressed air,
either of which may be used according to the position of the drill ,
e is the inlet hose with a stopcock, /drill-holder, g stretcher bar,
h piston, j rifled bar for turning piston and drill, k ratchet wheel
attached to rilled bar, I rifled nut fixed in the piston head, m wood
for lessening weight of piston rod and blocking space, n portway for
allowing the compressed air to pass to the top of the piston and give
the blow, 0 exhaust portway. The action oi the drill is as follows.
The compressed air is always acting on the underside of the piston,
and when the upper side of the piston communicates with the outer
atmosphere the piston moves rapidly backwards and uncovers the
portway n. The compressed air rushes through and presses against
the upper side of the piston, which has a greater area than the lower
sido, the difference being eijual to the area of the piston rod. The
piston is driven rapidly downwards and the drill stiikes its blow.
At the same time it uncovers the exhaust port o and then the con-
stant pressure on the annular area on the underside of the piston
produces the return stroke. The number of blows per minute is
from six hundred to eight hundred. The rotation of the drill is
effected by the rifled bar. On the down-stroke of the piston the
bar with fts ratchet wheel is free to turn under a couple of pawls, '
and consequently the piston moves straight whilst the bar and
ratchet wheel turn. A^ixen the up-stroke is being made the ratchet
wheel is held by the pawls and the piston is forced to make part of
a revolution. As the hole is deepened the cylinder is advanced
forwards by turning the handle p ; this works an endless screw q
^ Troc. Mining Institute o/ Cornwall, vol. i., 1877, p. 12.
448
MINING
TFOaMATION OP EkoiVATIOHB.
passing through a nut attached to the cylindar; r 13 the cradle
carrying the feed-screw and supporting the cylinder. It is centred
on the clamp 5. As this clamp can bo fixed in any position on the
bir. ind as t'-"' cradle can be turned on the clamp, it is evident
I .. nred in any direction.
In driring a level with the Darlington driU it is usual to fix the
stretcher bar horizontally across the level so as to command the
upper part of the face ; holes can then bo bored with the cradle
above the bar or below it. The bar is then shifted low enough to
bore the bottom holes. It is found that all the necessary holes can
bo bored from two positions of the bar. The bar therefore has
simply to be fixed twice ; the alteratior.s in position for boring holes
in various directions are managed by shifting the clamp on the bar
and turning the cradle on the clamp. Fig. 31 shows the stretcher
bar fixed in a vertical position, which is sometimes convenient.
In order to clear out the sludge from holes that are "looking
downwards, " a jet of water, supplied frora a hose attached to a half-
inch gas-pipe leading from a cistern at a higher- level, is made to
play into the holes during the process of boring.
For sinking shafts Jlr Darlington has the drul fixed in a cylin-
drical case with a large external thread which works in a nut on the
clamp. The drill is fed forwards by turning a hand-wheel attached
to the case.
Eotatiag Eotating machine driUs are aiso used in mines as well
drills, as those with percussive action. Stapff pointed out some
years ago that, if a rock may be chipped off by power com-
municated by a blow, it may also be chipped off by a similar
amount of power communicated by pressure. Brandt's
rotatory boring-machine consists of a hollow borer which
has a steel cro\vn with cutting edges screwed on. The
tool is kept tight against the rock by the pressure of a
column of water, and is at the same time made to rotate
by two little water-pressure engines, whilst a stream of
water passing down through the borer washes away the
ddbris and keeps the cutting edges cool. In principle,
therefore, this drill resembles the original diamond boring
machine of De la Roche-Tolay and Ferret, save that the
crown is made of steel and not of diamonds. During the
last few years it has been tried with success in railway
tunnels and in mines. Jarolimek's driU' acts also by
rotation, but the borer is fed forwards and pressed against
the rock by a differential screw arrangement. The machine
can be worked by hand, or by a little water-pressure or
compressed-air engine or an electro-motor. In working
certain minerals occurring in seams the undercutting may
be performed by machines similar to those used in coal
mines (see vol. vi. p. 68).
We now come to the application of the tools and machine
drills to the purpose of breaking ground for driving levels
and sinking shafts.
Driving A level or drift is a more or less horizontal passage or
levels, tunnel, whilst a shaft is a pit either vertical or inclined.
In driving a level by hand labour in hard ground, the first
thing the miner has to do is to take out a cut, i.e., blast
out a preliminary opening in the "end" or " forebreast."
The position of this cut is determined by the joints, which
the miner studies carefully so as to obtain the greatest
advantage from these natural planes of division. Thus
fig. 32 shows a case in which, owing to joints, it was
Fig. 32. Fig. 33.
advisable to begin with a hole No. 1, and then hore and
blast 2, 3, and 4 one after the other. The miner as a rule
does not plan the position of any hole until the previous
' Oeilcrreiehische Zeiischri/l /iir Berg- wid UMUnieetcn, 1881.
one has done its work; in fact he regulates the position
and depth of each hole by the particular circumstances of
the case. Though a vein and its walls may be hard, there
is ocasionally a soft layer of clay (DD, DD, fif;. 33) along
one ...^ (diy, Cornwall; gouge, United States). The
miner then works this away with the pick, and, having
excavated a groove as deep as possible, he can now blast
down the lode by side holes and so push the levo.l forward.
In sinking a shaft a similar method of proceeding is Sinking
observed. A little pit {sink) is blasted out in the most sh»ft».
convenient part, and the e-'icavation is widened to the full
size by a succession of blasts, each hole being planned
according to circumstances. This series of operations is
repeated, and the shaft is thus gradually deepened.
Where boring machinery is employed, less attention,
ancl^ometimes no attention, is paid to natural joints,
bec^^ when once the drill is in its place it is very little
trouble to bore a few more holes, and the work can then
be carried on according to a system which is certain of
effecting the desired result.
A common method of procedure for hard ground is Driving
shown in figs. 34 and 35. Four centre holes are bored '«*;?'»
about a foot apart
at first, but con-
verging till at a
depth of 3 feet
they are within
6 inches, or less,
of each other.
Other holes are
then bored around
them untU the ^^ =^^ ^'S- ^S-
Fig. 34
end is pierced by twenty or thirty holes in all. The four
centre holes are then charged and fired simultaneously,
either by electricity or by Bickford's instantaneous fuse,
and the result is the removal of a large core of rock.
The holes round the opening are then charged and fired,
generally in volleys of several holes at a time, and the level
is thus carried forward for a distance of 3 feet^ If the
ground is more favourable fewer holes are required, and
they may be bored deeper, — in fact as much as 6 feet in
some instances. Occasionally the four centre holes are
directed so that they meet at the apex of an acute pyramid,
and then, after all have been charged with blasting gelatin,
only one of them receives a primer and cap ; the shock of
the explosion of one charge fires the other three adjacent
charges simultaneously. The preliminary opening is not
necessarily made in the centue of a level, and sometimes it
is blasted out in the bottom or one side.
In sinking shafts by boring machinery operations arc conducted Sinking
much in the same way as in levels, save of course that the holes shafts
are directed downwards. Figs. 36 and 3/ are a section and plan of with
a shaft which is , ^
now being sunk at ^
the Foxdale mines
in the Isle of Man.
About forty-five
holes are bored iu
the bottom of tlic
shaft before the
drills are removed :
two of the holes
A, B, and occasion-
ally four, are bored
only i feet deep,
and arc blasted with ordinary fuse. They servo simply to smash
up ar.d weaken the core ; then the si.T holes nearest the centr*,
which are 8 feet deep, are blasted nil together with Bickford's
instantaneous fuse, and the result is tlie removal of a largo coro
leaving a deep sink. The remaining holes are fired in voUevs of
four at a time in the ordinary way. In this manner the sliaft,
which is in hard granite, is being deepened at the rate of 3J or 4
fathoms a month. Tonite is the explosive used.
Sundry machines have been in^-xjiitcd and used for driving levels
without blastiug. Some cut up the face into small chips which can
Fig 86.
F'g. 37.
PAYMBirr OP MINEES.]
MINING
449
feasfly be removed, but they have not made tlieir way at present
into ordinwy mining. The Bosseyense of MM. Dubois and rran9oi9
acts on a dMerent principle. It is a strong machine worked by
compressed air. It first of all drills holes i inches in diameter by
percussion ; a striking head is then substituted for the drill, and
wedges, on the principle of the plug and feathers, are inserted into
the holfcs ; and powerful blows with the striking head wodge off the
rock in lumps. ' This machine is being used with success in Belgium
for driving levels and crosscuts in fiery mines.
Some comparative experiments benreen hand-labour, a percussive
drill, and a rotatory dxill have -lately been made in one of the
Fieibarg^mines,' and the results are of much interest and import-
eince. The actual figures are as follows, the cost including, in the
case of the machines, interest, depreciation, and cost of repairs, and
cost of steam-power, supposing water-power not available :—
Hand-
boring.
Schram's
DHil.
Brandt-6
Drill.
ni » <lr1 n Tier week tin metres)
0-9.5
12010
120-5
1-S5 to
2-05
4-5
77-4 to
86-25
3-48 to
s-ee
8-0
74-34
3-76
UMjpe •
Wiges reallze4 bj the miners, in marks, per 8 1
hours shift — ■ i
The advantages of machine work are very marked indeed both
&3 regards rate and cost of driving, and wages earned by the men.
Brandt's rotatory drill did its work cheaper and &ster than Schram's
machine; but nothing is said in the original notice of the advantage
of a machine driven oy compressed aii- for ventilating workings such
OS advanced headings in which these drills are employed.
Brandt's machine was worked with water at a pressure of 83^
atmospheres, of which 56 '6 atmospheres were obtained by pressure
pumps provided with an accu-jiulator, and 26-9 atmospheres by
natural fall, owing to the working level being 277 metres below
the pumps. The water was conveyed to the machine in iron pipes
of 14 inches diameter inside. Tiie diainfiter of ^Y"^ hoin<i ^-.n^ff v.-^,^
SJ inches, and they could be bored in gneiss at the rate of IJ inches
■per minute. The stretcher bar on which the machine is carried
13 hollow, and has a piston which can bo forced out by hydraulic
pressure so as to fix the bar firmly. A similar bar is sometimes
used with percussive drills.^
As a method of breaking ground the ancient process of fire-setting
requires to be mentioned. Before blasting was kno-(vn it was lai^ely
employed, but its use is now confined to a few places on thj Con-
tinent where the rocks are exceedingly hard and where wood is
abundant and cheap. Piles of wood are heaped up against the face
of the workings and set on firs. On retumiug to the working place
two or three days afterwards, when the rocks h.ive cooled a little, it
is found that the ground has jplit and flaked off, arid''-..-t -"ic>. hrj
been loosened which can be removed by the pick and wedge.
"VTe finally come to water as an agent for removing rocks.
Streams of water were formerly used in South Wales for working
beds of clay ironstone at the outcrop. The water washed away the
clay and shale and left the clean nodules of ironstone. Tiie china
clay of Cornwall is also worked by water : a stream of water is
turned on to the soft mass, and the workman loosens the ground
with a pick; the water carries off the particles of decoicposed
rock in -suspension to regular settling pits. Water under pressure
has rendered vast services to the miner in working auriferous
alluvia. The system is described and figured at p. 746 of -vol. x.,
80 it is unnecessary here to enter into details. In the special case
of sal^mines recourse may be had to the solvent action of water,
directed by suitable jets, for making excavarions.
Vodesof 5. Principles of Employment of Mining Labour. — As a
P^ymg large proportion of the expenditure in mining is for actual
miners, mj^jj^^j labour, it is very important that means should be
taken to prevent any -waste in this department. Three
principles are in vogue — payment by time, by work done
either measured or weighed, and by the value of the ore
extracted.
The overseers, called captains in many metal mines, are
naturally paid by the month, and where strict supervision
can be exercised, such as is possible at the surface, on the
dressing-floors for instance, the same principle may be
adopted ; but when men are working underground, and
often in small gangs of only two or three persons at some
distance apart, piecework of some kind is more economical
and satisfactory in evei-y way.
In driving ievols and sinking shafts it is usual for the
* Jahrbitch fur das Berg- und IlUUenwesen im K^iigreiche Sachsen
Wif das Jahr 1882, p. 18, and abstract in Proc. Irtsl. Civ. £ng.,
vol. box., 1881-82, part UL p. 61.
' Annaks des Mines, ser, 8, ii., pL 1, fig. 8, 1882.
men to work at a certain price per running yard or fathom.
The agents have to see that the excavation, whether shaft
or level, is maintained of the full dimensions agreed upon,
and preserved in the proper direction. At the end of a
certain time, generally a month, the work is measured by
the agent. From the groM amount obtained by multiply-
ing the price by the number of fathoms driven or sunk it
is necessary to deduct the cost of the materials supplied to
the men by the mining company, such as explosives, steel,
candle.?, &c., and the remainder is divided among the
persons who took the contract. When the useful mineral
is being obtained the men may be paid at so much per
cubic yard or fathom excavated, or at so much per ton of
mineral extracted ; the overseer of course has to see, in
this latter case, that worthless rock is not sent to the
surface. Payment by the number of inches bored is a
method in use in some countries, where the men are not
experienced or enterprising enough to undertake the work
in any other way. A foreman points out to the men the
position and direction in which the holes must be bored,
measures them when completed, and subsequently charges
and fires them.
The third method is that which is known as the tribute
system. The miner working on tribute is aUowed to
speculate upon the value of the ore in a certain working
area assigned to him and called his pitch. He give.? the
mining company all the ore he extracts at a certain pro-
portion of its value, after he has paid all the cost of break-
ing ii, liciitiug it to the surface, and dressing it. Thus,
supposing he takes a pitch at 5s. in the £, and produces
marketable copper ore of the value of £50, his share -will
be 50 X 5s. =£12, 10s., less the cost of the materials he
has been supplied with, and aU expenses for -winding,
dressing, sampling, <tc.
6. Means of Securing Excavations hy Timber, Iron, and Timber-
Masonry. — The following kinds of timber are those most ""B-
frequently employed for secoring excavations underground :
oak, larch, pitch pine, spruce fir, and acacia. In many
::r::;?s the timber is attacked by dry rot, -rthich gradually
renders it useless, and when the timber has often to be
renewed the expense may be very considerable. Various
methods of pi^venting dry rot have been tried -with more
or less success, such as letting water trickle over the timber
in the mine or treating it -with preservative solutibns
beforehand. Brine, creosote, and solutions of chloride of
zinc, sulphate of zinc, sulphate of copper, and sulphate of
iron increase the d oration of timber. It was found by
experiments carried on at Commentry during a long series
of years that one of the best plans was to soak the tiiilber
for twenty-four hours in a strong solution of sulphate of
iron. The total cost was only Jd. per yard of prop, -u-hilst
the timber lasted eleven times as long as when this simple
treatment was omitted.
Timber is used in various lorms — either whole and merely
s.iwn into lengths, or squared up, or sawn in half, or sawn
into planks of various thicknesses.
Where the roof of a bed is weak it may be kept up by simple
props ; but in some coal-
mines and clay-minesabetter
support is obtained by logs
{chocks) laid two by two
crosswise (fig. 38).
Though a level is an ex-
cavation of a vei-y simple
nature, the methods of tim-
bering it vary considerably,
because the parts requiring ^ .^. ,,.
support may either be the ^ -j j
roof alone, or the roof and one or two sides, or the roof, sides, and
bottom. ■ /. , J v i_
If the roof only is weak, as is the case with a soft lode be^eei
two hard walls, a cap with a few boards resting on it (£g. 89) is
sufficient to prevent fails. If one side is weak the cap must to
^ XVL — 57
Fig. 3S.
450
MINING
CURING EXCAVATIONS.
supported by a side prop or Ug (fig. 40), ana very often by two
legs. The forms of joint between the cap and leg are numerous
Fig. 3?. Fig. 40.
(fig. 41), depencUug to a great extent upon the nature of the pres-
sure, whether coming upon the top or sides. With round timber
the top of the leg is
«ometimes hollowed
t3 shown in fig. 42
A, but occasionally
the joint is flat and , .
a thick nail, or nog, -^ ^
is put in (fig. 42 B) ^ Fig. 41. Fig. 42.
to prevent the effects ci side pressure, or, better, a piece of thick
plank is nailed under the cap (fig. 43). Where the floor of a level
is soft and weak, a
sole-piece or sill be-
comes necessary, and,
if the sides or roof are
likely to fall in, a
lining of poles or
planks is used (iig. 43).
In some very heavy
ground in the Cora-
stock lode a special
Xpted(fi^«r" ^**^- . ^'^■''-
If the ground is loose, so that the roof or sides, or both, will run
in unless immediately supported, the method of working called
filling or poliitg is pursued. It consists in supporting the weak
parts by boards or poles kept in advance of the last frame set up.
The poles or boards
{laths) are driven
forward by blows
from a sledge, and
the ground is then
ivorked away with
the pick; as soon as
a, sufficient advance
has been made a new
frame is set up to
support the ends of
the poles or boards
and the process is re-
peated (figs. 45 and
46). In running grouna it is necessary to have the laths fitting
closely together, and the working face also must be supported by
breast-hoards kept iu place by little struts resting against the frame.
These are removed and advanced one by one after the laths in the
roof and side have been driven beyond them.
Iron On account of the high price of timber, iron is sometimes em-
supports, ployed in its place. One method
in use in the Harz consists in
bending a rail into the form
shown in fig. 47 and making it
support other rails laid longi-
tudinally, against which flattish
stones ara placed; the vacant
spaces are then filled with
rubbish.
Jlasoniy. Masonry has long been used for
supporting the sides of mining
excavations. The materials
necessary aro stone, ordinary
bricks, or slag-bricks, and they
may bo built up alone (dry
V}aili7ig) or with the aid of
Figs. 48 and 49 show me&ods of securing a diift by arches when a
lode has been removed.
The timbering required for shafts varies according to the nature Timbd
ingfor
shafts.
Fig. 45. J- ]g. 4y.
of the ground and the size of the excavation. A mere lining
of planks set on their edges (fig. 50) suffices for small shafts,
corner pieces being nailed to keep the successive
frames together. In some of the salt-mines of
Cheshire the shafts are lined with 4-ineh planks
united by mortice and tenon j'oints.
The usual method of securing shafts is by
sels OT frames. Each set consists of four pieces, Fig. 50.
two longer ones called wall-plates and tvvo shorter ones called erxd-
pieces. They are joined by simply halving the timber as shown in
Fig. 45.
><-^^-
Fig. 47.
mortar or hydraulic cement. The bottom of a level is occasionally
lined with concrete to cany a largo stream of water, which other-
wise might run into lower workings tlirough cracks and crevices.
Dry walling is not uncommon, and it may be combined with the
use of timber (or iron) as shown iu fig. 69, in which a level is
maintained between two walla keeping back a mass of rubbish.
Fig. 51. Fig. 52.
fig. 51, A more complicatea joint (fig. 52) is often prefen-ed. The
separate frames are kept apart by corner pieces {studdles, Cornwall J
jogs, Flintshire), and loose ground is prevented from falling in by.
boards or poles outside the frames.
As shafts are frequently used for the several purposes of pumping,
hoisting, and affording means of ingress and egress by ladders, it
becomes necessary in such cases to divide them into compartments.
Pieces of timber parallel to the end-pieces {huntoTis or dividings)
aro fixed across the shaft, and serve to stay the wall-plates and
carry the guides as well as to support planks (casing boards) which'
are nailed to them so as to form a continuous partition or.
brattice. The magnificent timbering of some of the shafts on thq
Comstock lode is described by Mr James D. Hague as follows : *— ^
*'The timbering consists of framed sets or cribs of square timber,
placed horizontally, 4 feet apart, and separated by uprights or posts
introduced between tliem. Cross-timbers for the partitions between
the compartments form a part of every set. The whole is covered
Fig. Ii4. Fig. 55.
on the outside by a lagging of 3-inch plank piaeed vertically. " Figs.
53, 54, and 55, copied from Mr Hague s plates, illustrate this method
0/ the fortieth I'arallcl, voL lU^
iZZPLOITATIOK.]
MINING
451
of timbering. Fig. 53 is a dUb of the shaft: " 3, S are the longi-
tndioalorSl-timbers, T, T flie transversa end-timbeis, P portition-
timbeis, r gaide-rods between which the cage mores, g eaina cat
in the sill-timbera, to leceive the ends of the poets. The sheathing
or lagging is seen enclosing the whole fiame. ' Fig. 54 is a tians-
Teiso section through the partition P of fig. 53, "between'the
})nmping compartnient and the adjoining hoisting compartment,
ooking towards the latter. In this figure, G, G are the posts, S
the rifl-timber^ P the partition-timbers, the ends of which are
framed with short tenons that are received in gains cut in the sill-
timbers and the ends of the posts, r guide-rod, I lagging or
sheathing." Fig. 55 is an end view of the frame shown in fig.
63. "The single piece T forms the end, while the doable pieces P
forming the partitions are seen beyond." **The outer timbers of
each set, that is, the two sides and ends of the main frame, are
14 inches square ; the posts, ten in number, four at the comers
and two at each end of the tiiree partitions, are of the same size.
The dividing timbers, forming thepartitions, are 12 inches square."
"When ground is loose or running, recourse must be had to a
tpilling process like that described for levels. Strong balks of
timber are fixed at the surface or in solid ground, and then the first
£rame is hung from these bearers, and each successive &ame from
the one above it. Iron bars with cotters may be used for suspend-
ing the sets ; but on the Comstock lode each bolt is made, in two
parts with a tightening screw in the middle, and the sets can thus
be kept very firmly together. The laths are driven in advance, in
the manner explained in the case of levels, and a new frame is put in
as soon as the excavation has been sufficiently deepened within the
protecting sheath of boards. In vary unstable ground it may bo
necessary to put iti the frames touching each other, so that the
shaft becomes encased in a solid box of timber, occasionally H inches
thick.
Like levels, shafts may be lined with masonry or brickwork, and
^^■7 these have the advantage of being far more permanent than timber,
*^ and of requiring fewer repairs. This kind of shaft-lining is
especially desirable in the loose ground near the surface; because, if
the working is discontinued temporarily, the shaft still remains
secure and available for use at any future time, whereas if timber is
put in it often decays, the top of the shaft collapses, and much ex-
pense is incurred in the process of reopening it. The section of the
shafts that are walled is generaUy circular as afibrding the best
resistance to pressure; but elliptical walling is also met with.
Another shape is like a rectangle, save that the sides, instead of
being straight, form curves of large radios. The waling may be
dry or with mortar, according to circumstances.
The masonry is put in either in one length or in successive por-
'tions in descending order, and this is the usual plan. The shaft
is sunk a certain depth, with temporary timbering if necessary,
and when firm ground has been reached a bed is cut out round
the shaft, and on this is placed a crib or curb AB (fig. 66'^ con-
sisting of segments of timber which form
a ring. This serves for a foundation for
the brickwork, which is built up to the
surface; the temporary timbering is re-
moved, and the spacefilled up with earth
or concrete. Sinking is then resumed
below the curb, and for a certain distance
of a smaller diameter, so as to leave a
bracket, or ledge, to support the first curb.
On arriving, after a cer&in depth of sink-
ing at another firm bed, a second cnrb
CD is put in and a portion of brickwork
built up. ^Vhen the ledge of rock is
reached^ it is carefully removed in small
sections and the brickwork brought up
to the first curb. This process is repeated
till the shaft is completed, or reaches rock
in which no masonry is requisite. If,
owing to the nature of the ground, it
is impossible at first to find a firm seat
for the curbs, it becomes necessary to hang Fig. 6S.
them by iron bolts from a strong bearing frame at the'Soiiaea.
VThen shafts pass through very watery strata, it is most desirable
to stop all influx into the mine for the purpose of saving the
heavy expense of pumping. The manner in which this is effected
by a watertight lining. Known as tubbing, is described in the article
Coal, voL vi p. 62, where will also be toondan account of Trigcr's
plan of sinking shafts with compressed air, and the very successful
method of boring shafts through water-bcsjing ground invented by
Messrs Elind & Chaudron.
oi- 7. Exploitation, or WorJcing Away of Veim, Beds, and
^ Masses. — We have described how shafts are sunk and levels
driven, and we now come to the processes employed in
removing the mineral.
^ J. Gallon, Lectures on Mining, toL L, Atlas, plate xxviii.
The deposit most first of all be reached by a shaft, or,
where the coatour of the country permits it, by a leveL
In the case of a vein an exploratory shaft is often sunk oa
the course of tLe lode for 20 or 30 fathoms, and, if the
indications found in a level driven out from this shaft
warrant further prosecution of the mine, a first working
shaft is sunk to intersect the lode at a depth of lOO
fathoms or more from soo™.
the surface. Crosscuts
are then driven out at
intervals of 10, 15, or 20
fathoms to reach the lode,
as shown in fig. 57, which
represents a section at
right angles to the line
of strika Sometimes the
main shafts are carried
down all the way along
the dip of the deposit,
though perpendicular
shafts have the advan-
tages of quicker and
cheaper winding and
cheaper pumping, to say ^- ^7.
nothing of the possibility of utilizing the cages for the rapid
descent and ascent of the miners. If an inclined shaft
appears to be advisable, great care should be taken to sinli
it in a straight line. In either case levels are driven ont^
along the strike of the lode as shown in the longitudinal
section fig. 58, in the hopes of meeting with valuable oid-
7~ ' ' ^^"~
Fig. 68.
bodies such as are represented by the stippled portions of
the figure. For the purpose of affording ventilation, and
still further exploring the ground and working it, inter-
mediate shafts, called vritues (Cornwall) or sumps (North.
Wales), are sunk in the lode.
The actual mode of removing the lede itself d^ends a good
deal upon circumstances, viz., its width, the nature oi its contents,
and the walls that enclose it ; but the methods of working may
generally be brought under one of two heads, viz., underhand
■toping or overhand stoping. The word slope is equivalent to
step, and the term stoping means working away any deposit in a
series of steps. Underhand or hcUorn slopes are workings arranged
like the steps of a staircase seen from above, whilst ovfhcmd or
back slopes are like similar steps seen from underneath. Both
methods have their advantages and n-rTTj},
disadvantages, and both ai« largely ///f/f/t
used.
Wo will first take underhand stop-
ing, as this is the older metlic -
In the old days the miner began
the floor of the level (fig. 59), r.; .
sank down a few feat, removing the
part 1 ; he followed with 2, 3, 4, tc, --o— •
until the excavation finally presented the appearance shown m
fig. 60. Any valueless rock or mineral was deposited upon nlat-
forma of timber (siujb), and the ore was drawn up into the Jevsl
452
MINING
[bstloitation.
by a windlass. One great disadrantaga of ttu mctliod is that tlia
ore and water have to bo dra \n up lu li it ' ujl labour;
much timber is required ^ ^
for the stulls if there /> ^ /A//^f//
is a largo quantity of -'■ ^ — ' — "
y/orthless stuff in tha
vein, or if the sides aro
weak. The advantages
are that ore can ba
■worked away as eoon as
"the level is driven, that
the men are always bor-
ing downwards, and,
lastly, that the ore can Fig. CO.
be carefully picked after it is broken, without fear of any valuable
particles being lost.
A more economical method of working by underhand stopes, and
«ne largely employed in Cornwall at the present day, consists in
reserving any attack upon t i i i / ■ / i 1 1 i > i i ,
the era-ground untU a lower // // ////////7/////
level ms been driven. An ■' — ^ — ' — ' — -t-i— t-fc-t
intermediate shaft {wintt)
between the two levels is
then made, either by sinking
from the upper level or rising ,
from the lower one. The /
"work of sloping is com- "f^'"^''.'fnp~^;i3^S5*E:'^'^"~'^"'^ ^"^
menced at the two upper / / / // 77/77 ///////
ends of the winze, and the / / /////// // / ///>
lode is removed in a sv.c- Fig, 61.
<;ession of steps, the workings assuming the appearance exhibited in
fig. 61. The stops are generally made Steep, so that the ore may
leadily roll into the winze, and so that the boro-holes may do better
esecution; but these steep stopes are daugerous if a man happens to
slip and fall. The huge open chasms left by the removal of a large
loda in this way are also a sourco of danger ; for there is always a risk
of falls of rock, and from places which cannot easily be examined.
Figs. 62 and 63, kindiy supplied by Captain Josiah Thomis,*
explain the general arrangement of the workings of the largest
tin mine in Cornwall. The lode after producing copper ores to
a considerable depth changed its character and became rich in tin.
The workings for tin ore are confined almost entirely to the
granite. The section fig. 62 shows that the main shaft of the mina
13 at first vertical and then carried down on the dip of the lode.
SOUTH
V
Fathoms 100 su 0 100 Fs'.!iom,
Fig. 62. — Transverse Section, Dolcoath Mine, Cornw.ilL
The process of overhand stoping is precisely the reverse of that
Otot-
iiatid
dtopb!;.
I I I ! I I I I I I I I Scale.
Fatboms
Fio. ^Z. — Longitudinal Section, Main Lode, Dolcoath Mine, CorawalL
•which has been just described ; the work is commenced from a rise I (fig. 64 A), or better from the two bottom cuds of a
As soon as the men have excavated a sufficient )ici
I the level, they pnt in strong pieces of timber from
4*0 'Tathoma.
winze ifig. 64 B).
;;lit of the roof of
wall to wall, and
EXPLOITATIOX.]
MINING
453
cover these cross-pieces {sicmpeh, slull-piccei) with boards or poles,
and throw down the rubbish upon the platform (stull, hunning)
thus formed. In the midst of the rubbish chimney-like openings
{mUU, paaets) are reserved, lined with boards or dry-walling, and
W77ZyZ^777/777P7T7
Fig. 66.
Fig. 64.
closed at the bottom with shoots provided with doors. The ore
id thrown into these passes, which are tapped when necessary; the
ore falls into the tram-waggon placed ready to receive it.
Fig. 65 gives a transverse section showing the rubbish resting on
the stall. This is what may be called the typical method of stop-
ing, when the lode affords rubbish enough for the men to stand on
and to keep them close to the rock they are attacking. Very often
such is not the case, and the whole of the lode has to be sent to the
eurface for treatment. If the v/alls are firm, the lode is sometimes
stoped away, a stull put in, and a sufficient heap of broken ore is
left upon the stull to give the men good standing ground ; the excess
is thrown over the ends of the stull, or the great heap is tapped by
st^Uove*ring/and ^al- \ n\\\ ^ ^ \\\\\\\\\\\\\
lowing a quantity to
run down into the level.
Another method con-
sists in putting in
temporary stages upon v ■
which the men stand to \-^
do their work, whilst
the excavation is left as
an open space (fig, 66).
This mode of working is incompatible with weak walls. If a lode
does not afford rubbish enough for coi^plctely filling up the
vated space, or if it is too narrow
for men to do their work comfort-
ably, one of the walls may be cut
into and blasted down (fig. 67), so
that the men always stand upon a
fimi bed of rubbish while at work,
and there is no fear of a collapse
of the mine. In certain special
cases rubbish is sent down from the
surface to fill up the excavations.
The advantages of overhand
stoping are — that the miner is
assisted by gravity in his work,
that no ore or rock has to be drawn
up by hand labour, and that less
timber is required. On the other
hand, the miner is always menaced _.
by falls, but as he is close by he *'^S- ^7.
can constantly test the solidity of the roof and sides by sounding
them with his sled je ; there is the further disadvantage tljat particles
of ore may be lost in the _
riibbish, but this loss
often prevented by laying ^;^
down boards or sheets of ^:^
iron while the lode is being "^
broken down.
Working "When very mdo lodes
wide come to be worked, recourse
lodes is often had to special
methods. The great lode
V.^a at the famous Van mine, in
mine. Montgomeryshire, is some-
times 40 feet in width, and
the hanging wall is weak.
The lode is stoped away
overhand, and the cavities
packed with rubbish, part
of which is derived from
the lode itself, whilst the
greater portion is supplied from a special quarry at the surface.
Fig. 68 ^ explains the details of the case. A is the original cross-
i tbe Van Mine," TroM, Rq». Oeol. Soc. Con>
Fig. 6&
cut (not in the line of section) by which the lode was reached,
B is thejluean, C the bastard lode, generally worthless, E the main-
lode, Hperraar^iitlevels, and K ore-j3(W5 reserved amidst the rubbish
(deads) D, I pass du-;-ra which rubbish is shot, N crosscut connect-
ing the level H with P the permanent level in the coxcnlry.
If the lode is not firm enough to allow of the stopes being carried
for its full width, the crosscut method is adopted ; the workings
in this case, instead of proceeding along the strike, are carried across
the deposit from one wall to another.
The lode is removed in successive horizontal slices ABODE-
and for each slice a level (L, fig. 69) is driven, either in' the'lod^
1 >o >■ ^ Fig. 70.
01 partly or entirely in the country; from this level crosscuts arc-
put out 6 or 8 feet wide, as shown in the plan (ng. 70). These are-
regularly timbered accoiding to the necessities of the case, and,
when No. 1 is completed, No. 2 is begun, and the rubbish from
No. 2 thrown ii.to the empty space of No. 1 crosscut. If the
quantity is insufficient, deads are brought in fk>m the surface or
from exploratory workings in worthless rock in the neighbourhood.
Sometimes the crosscuts are not driven side by side, but 1 and 5
would be di-iven first, leaving 2, 3, and 4 as a solid pillar ; then 3
would be worked away, and finally 2 and 4 between the timber and
rubbish on each side. The greater part of the timber can be re-
covered when the next slice above is taken ofi", as the props are put
in with the small ends downwards, and- can bo drawn up with
levers. M (fig- 69) is a level reserved in the deads for traffic and
ventilation. This method of working is applicable not only to
lodes but also to iiTegular masses.
In working away the soft '* bonanzas " or ore-bodies of the great Comrt*^
Comst«ck lode, which are from 10 to 30 or even 40 or 50 feet wide, lodt.
and which are enclosed in very un-
stable ground, a special method of
timbering is employed (figs. 71 and
72).- " It consists in fiiaming timbers
together in rectangular sets, each set
being composed of a square base
placed horizontally, formed of four
timbers, sills, and cross-pieces, 4 to
6 feet long, framed together, sur-
mounted by four posts 6 to 7 feet
high, at each corner, and capped by
a frame-work, similar to that of the
base. These cap-pieces, forming the
top of any set, are at the same time
the sills or base of the next set above,
the postsj as the sets rise one above
the other in the stope, being gene-
rally placed in position directly over
those below." "The timbers are
usually of 12-inch stuff square-hewn
or sawn." Each post has a tenon 9
inches long at the upper end, and a
tenon of 2 inches at the lower end,
which fit into mortices in the cap
Fig. 72.
id sill respectively; and "the
sills and caps have short tenons on each end and shoulders cut to
receive the ends of the post and the horizontal cross pieces." The
walls of the excavation are sus- ,
tained by a lagging of 3-inch
or 4-inch plcnk. The whole
width of the ore-body is stoped
away at once, and its place
supplied by timbering, and
finally the vacant space is filled
with waste rock derived froi^
dead work in the mine or fr:'
special excavations, — undi; r
ground quarries in fact, — in L^..^i^ j^>\.u..vl. T..^ ^.-^ ..._,:-.------
on overhand, starting from an interDiediate shaft or v.iu/e, and fig.
73 will exnkun how the different frames are built up one above the-
other.
Another metfiod of working a wide lode is to attack it in slices
Iffl
ipHPHI
y
T ^
in.
ms :^-
United S(a(e% Geological Exploraticn o/ the PortUth
;»ins Industry," p. U2.
454
MINING
[exploitatioh.
parallel to tho dip, working away each slice separately as if it were
a lode of ordinary dimensions, and filling
up with rubbish (6g. 74).
jWorking We now come to Deds or seams. The -
•jf beds, mode of working the most important beds
that occur in the earth's crust, viz., coal
seams, has already been described in the
article Coal (vol. vi. p. 64 sq.), and
details have been given concerning the ^
removal of the mineral by pUlar working ^v'
and long-wall working. Both these ^^
methods are applicable in tha case of ^^
seams of other minerals. Such for ^*^
instance are the beds of fireclay and
•clay-ironstone which are wrought by ^'8 '*
both the processes just mentioned, and often in connexion mth coal
Next in importance to coal is ironstone, and a brief account of
the workings in the Cleveland district will explain the manner in
which more than one-third of the iron ore raised in the British Isles
is obtained by mining. It resembles the ' ' bord and pUlar " system
used for working coal in Durham.
ia«T6- The Cleveland ore occurs in the fonn of a bed from 6 to 18 feet
land thick in tho Middle Lias, lying pretty level. A mainway (fig. 75)
ironstone is driven about 1 2 feet
work- ■wide for a considerable
■■ilga. distance, and at right
angles to it bords are
driven 5 yards wide for a
length of 30 yards, and
then at right angles a
wall 7 or 8 feet wide and
20 yards long. By driv-
ages of this kind the bed I
is cut up into pillars or "H T
Wocks 30 3'ards lopg by
20 yards wide, The
pillars are subsequently
removed in the following
■way. A place, or drift,
ab, 6 feet wide, is driven Fig. 75.
across' the pillar 10 yards from the comer, and. portions (lifts) about
6 yards wide are worked away in tho order 1, 2, 3. After No. 1 lift
lias been removed, the timber put in to support the roof temporarily
'^ y'^T '?'^' ,^°'' *^ ^°°^ '=> allowed to fall ; No. 2 is then taken,
and No. 3 in the same way. While these Ufts are being taken out
another place erf is being driven across the pillar 10 yards from the
""',• an'' the pillar removed entirely by a series of fresh Ufts.
^'''°™ Al^' '°/''V^<'^eati m section and plan the chambera and pillars
^oames. ot the underground gypsum quarries
which sipply the well-known plaster
of Paris to all the world.' The
principal bed is from 60 to 60 feet in
thickness ; pillars are left 10 feet
square at the base, and the stalls
between them are 1 6 feet wide. The
■workings are slightly arched, and are
not carried up to tho roof, for the
purpose of better maintaining the
security of the chambers, because
heavy damages would have to be
paid if they "caved in" and ren-
dered tlie surface useless. A simi-
lar layer left for the floor prevents
creep (see Coal, vol. vi. p. 64), and ^'8- "6-
enables the underground roads to be kept in good repair.
Underground slate quarries afford examples of very various
I. methods of removing thick beds of mineral of comparatively little
intrinsic value, At Angers in France, where the beds dip at a high
angle, the Uiidorground workings are carried on like an openquaiTy
Festiniog district in North Tyales the principal bed, or vein as it ia
called, is more than 100 feet thick in places, and the method of
working consists in making alternate pillars and chambers each 30
feet to 50 feet wide along tne strike (cross-iection and plan, figs. 77
and 78). Tho pillars follow lines of natural cross-rending PP', which
commonly make an angle of 25° to 35° with the direction of the dip.
The excavations are arranged in regular lines, and form continuous
chambers extending very often from the surface to tlie very lowest
workings. A,B,C,D are theoriginal working levels. Theslateofthe
supporting pillars is entirely lost, as these cannot be Venioved with
safety. This method of working requires a strong roof. In the
Ardennes, on the contrary, the pillars are carried along indefmitelv
along the strike (fig. 79, cross-section). The slate in each iongi-
tudinal chamber is removed in slices parallel to the bedding, and
the men stand upon tho rubbish, which finally fills up the chamben
completely.
Rock-salt constitutes another important mineral which occurs in „
tho form of stratified deposits. The principal source of the Cheshire ^' '
salt 13 a bed 84 feet thick lying horizontallv; but only the bottom
part, 15 feet to 18 feet thick, is mined. Pillars 10 yErditquare arc
left promiscuously about 25 yards apart, as shown iu lig. 80, whici
represents part of Maiston Hall rock-salt mine.^ The working
□ Q
a
SUte
guarries.
Fig. 77.
Fig. 78.
Fio. 79. —A, A,
pillars of slate ;
B, B, rubbish ;
■C,C,slatecham-
bcrs-Scaley^jj.
under a trong roof of slate ; the floor is continually being worked
away in steps, and an immense open chamber is left. In the
1 CalloD, Lecturet on Hining, vol. U. plate xU,
Fig. SI.
are advanced by making in the upper part an excavation 5 feet C
inches high, called the roofing [a, fig. 81); and then the lowci
two-thirds of the part worked are removed by blasting slanting
holes. Many of tho old salt mines have collapsed from weakness o;
the roof or insufficiency of the pillars, and have become inundated
the brine is then extracted by pumping and evaporated for salt
In some countries, especially when the beds of salt are impure oi
much mixed with clay or shale, the formation of brine is conducted
regularly by making a network of drivages within a rectangular,
elliptical, or circular area in thick beds of saliferous marl, and then
introducing fresh water by pipes, so as to form underground pondi
which gradually dissolve the roof and sides. The brine is drawr
off and either pumped up or conveyed by adits to the surface.
A few words remain to be saiS about open workings. Somt
minerals are always obtained in this way ; others are worked oper '^^ "^
before regular underground mining begins; and, thirdly, it olteu "-floWP
happens that underground and surface work are both carried on
simidtaneously on the same deposit. Among deposits worked open-
cast are peat, numerous kinds of stone, iron ore, cupreous pyrites,
lead ore, gold- and tin-bearing alluvia, and diamontiferous rock.
Owing to its soft, spongy, and fibrous texture, and tho fact of ita
often lying below the water-level, peat has to be worked in a
special manner. Trenches are dug about a foot deep with* sharp
spade, which cuts out sods of convenient size for drj-jng and burning.
When one layer has been removed in this way, another is taken oil*,
and so on. If \vater is reached the working can still iie pursued by
using the long spade (grand louchet, France) with a hsndle of 16 or
20 feet It cuts out a so^ 3 or 4 feet long at each thrjst.
■When a deposit is more or less solid the workingj are frequently
arranged in steps, the height and breadth of each depending upon
the firmness of the rock.
In many cases the first work consists in removing worthless rock
at the surface (overburden), and where the underlying deposit is
thick or very valuable it will pay to remove a veiy great thickness
of overburden, on account of tho advantages of working a deposit
open. These advantages are — entire removal of the deposit witnouf
loss in pillars, no expense for timbering or for packing with rubbish
or for ventilating or lighting che workings, better
ventilation, easier supervision, longer working hours,
less danger.
As an example of a largo open wcking may be
mentioned the groat Fenrhyn slate quarry near f
gor, employing about 3000 hands, jind worked by a
succession of terraces on an average CO feet high by
30fcetwide(fi2. 82). Reference has ali-csdy been made |
to tho thick lead-bearing sandstoue of >Jechornich,
which is in part worked as an open quarry. Mokta-cl-
Hadid, near Bona in Algeria, and the Kio Tinto mines
in Spain, afford instances of extensive combined open and under-
ground workings for iron ore and cupriferous pj-ritcs respectively.
Local laws regulating tho size of the working areas, or claim's.
Fig. 82.
CARKIAOB.]
MINING
455
Diamond
Evils at-
tcn<ling
hy.
draul:c
minmg.
Under-
ground
trans-
port.
Carriage
by
Slci,?'-!.
"Vheel
carriages.
owned by Mparate indiTiduak or companies, considerably affect the
methods of working- This is especially the case with the diamond
deposits of South Africa. The diamantiferous rock at the celebrated
Kimberley mine (formerly called Colesbcrg Kopje) occurs in the
shape of an elliptical upright mass, the greatest length being about
330 yards and the greatest breadth about 200 yards. The super-
ficial area is about 9 acres; the mass extendsdown wards within almost
perpendicular walls of shale, and is worked in places to a depth of
about 400 feet. The claims are only 31 feet sfjuare, and are more
than four hundred in number, and these have in some instances been
subdivided iuto portions as small as the sixteenth of a claim; but,
as at the present time one company may own very many claims, the
number of individual holdings is less numerous than formerly when
the limit was tw» claims. The working is carried on vertically
downwards, and, as the claims are not all worked at the same rate,
those that progress most rapidly are surrounded by perpendicular
walls of neighbouring claims. The shale, or rztf^ enclosing the
deposit is constantly falling into the huge open pit, and has to be
cut away to a slope, the expense of this work being charged to the
claim-holders generally by the mining board. The diamanti-
ferous rock is extracted by innumerable \vire-rope inclines.
We have already referred to the method of workin" gold-bearing
alluvia by the hydraulic process, which has rendered such services
in the United States (Gold, vol- i. p. 746). At the same time one
must not be blind to the evils of this method of working, which have
at last necessitated legislative interference. Some idea of the extent
of the mischievous results of hydraulic mining will be gathered from
the statement that one working alone, the Gold Run Ditch and
Mining Company, for the last eight years has been discharging 4000
to 5000 cubic yards of sand, gravel, and boulders daily, for a period
of five months each year, into a tributary of the Sacramento. As a
natural consequence deposits are formed lower down the river, ob-
structing the navigable channels, rendering overflows more frequent
and destructive, and causing valuable land to be destroyed by de-
posits of sand. The superior court of Sacramento county, California,
Las recently decided that the hydraulic minin<^ companies must
build dams to impound the coarse and heavy debris, or take other
cCKcacious means to prevent their being washed down the rivers.
8. Carriage or Transport of Minerals along the Under-
ground Roads. — After tte mineral lias been broken down
ia a deposit it is necessary to pick out any barren rock and
then convey to the surface all that is of value.
The simplest and oldest method of transport along
underground roads is carriage on the back, and this method
may still be seen at the present day even in countries
where the art of mining is generally highly advanced.
Thus, for instance, in the little slate mines near Cochem
on the iloselle men and lads carry up all the blocks of
slate upon their backs, walking upon steps cut in the rock ;
they come up with their hands upon the ground bent
almost double under the weight of the block, which rests
upon a thick pad. Again, the blocks of slate are stUI
carried on the back from the actual working place to the
nearest tram-road, in the slate mines of the Ai'dennes. In
the Sicilian sulphur mines the same method is common,
and it is found also in parts of Spain and China, where
baskets are used, whilst bags are employed in Mexico and
also in Japan. Even in England the system still survives
in the Forest of Dean, where boys carry iron ore in wooden
trays from the very irregular ore-producing cavities either
to the surface or to the nearest shaft.
Sledges, or sleds, enable greater loads to be transported ;
but they are not available unless the conveyance is along
roads sloping downwards. They have been largely
employed in coal mines, and are still resorted to in some
collieries for conveying the coal from the working place to
the nearest tram-road.
We next come to wheeled carriages. The simplest is the
wheelbarrow. The barrow used in Cornwall at the present
;lay is not unlike that figured more than three centuries
ago by Agricola. The navvy's barrow is more advan-
tageous, but it requires a wider and higher level. The
barrow runs upon the natural floor of the level, upon
boards, or upon thin strips of iron. Carts dravm by horses
may be used in large underground quarries. Excepting in
special cases it is advisable to replace barrows by waggons
running upon rails. The oldest form is the German Hund.
It consists of a rectangular wopden body, with four wheels,
resting upon two boards as rails, and it is kept on tha
track by a pin which runs between the boards.
Cast-iron tram-plates were introduced in the last century,
and were finally succeeded by iron rails, which are now ia
general use, though steel threatens to displace iron in this
as in other departments of mining. Various forms of rail
are employed. The simplest is a bar of iron set on its
edge in transverse sleepers, or flat iron nailed to longitudinal
sleepers. Small T-headed and bridge rails are not
uncommon. In the Harz the rails sometimes lie on stone
sleepers ; a hole is bored in the stone, plugged with wood,
and the rail is nailed on. The gauge varies from 14 inches
to 3 feet or more ; 20 inches to 22 inches is a common gauge
in metal mines. Arrangements of course have to be made
for passing from one line to another by points ; but the
transference is frequently best effected by putting down flat
plates of cast iron, upon the smooth surface of which the
waggons can be handled with ease and turned in any direc-
tion ; raised ledges guide the wheels into any particular track.
The form and size of the waggons running upon the rails
necessarily vary according to the size of the underground
roads and the manner in which the mineral is raised in the
shaft. In some mines the practice exists of loading the
mineral in the level into an iron bucket (k-ibble) standing
upon a trolley, which is merely a small platform upon
wheels. This trolley is pushed (trammed) to the shaft ;
the full kibble is hooked on to the winding-rope and drawn
up, whilst an empty kibble is placed upon the trolley and
trammed back along the level, where it is again loaded
from a shoot (mill, pass) or by the shovel. The usual plan,
however, is to have a waggon, which is tipped on coming
to an enlargement of the shaft (plat, lodge) where the level
joins it. These waggons may be made of wood or sheet-
iron, and of late years sheet-steel for the body and cast-
steel for the wheels have been coming into favour.
The most modem system in metal mines is to imitate
collieries, and use waggons which are drawn up in cages.
Fig. 83 represents the plain but strong waggon of the Van
mines, consisting of a rectangular
body of sheet-iron resting on an
oak frame, and provided with
cast-steel wheels. The wheels are
loose upon the axles, which them- C
selves run loose in the pedestals.
The waggon is emptied by being
run on to a " tippler," which enables it to be completely over-
turned with great ease. A commoner plan is to construct
the waggon with a hinged door at one end, and the contents
are discharged by opening this door and raising the body.
The motive power for tramming waggons along the levels of
metal mines is generally supplied by men or boys, though, where
large quantities have to be extracted, and where the roads are
favourable, recourse may be had to ponies and horses and the various
kinds of mechanical haulage described in Coal, vol. vi. p. 69. '
Trains of cars are sometimes drawn along imdergrouna railways
by locomotives ; they have the great disadvantage of polluting the
air with the products of combustion, and consequently they are not
available unless the ventilation is very good. A small locomotive of
2 horse-power nominal is tised on an IS^-inch track in the adit-level
of the Great Laxey mine (Isle of Man), now approaching a mile in
length, and full-sized locomotives ply along the adit of the Rio
Tinto mines. Locomotives worked by compressed air improve the
ventilation instead of injuring it, and are not a source of danger in
cases where fire-damp may be present ; but, except in special cases,
they cannot be worked so cheaply as engines fired with coal. Con-
veyance by electric railroads underground has hardly gone bej'ond
the experimental stage, but the results obtained at the Zaukerodt
colliery in Saxony' show that electricity can be applied with profit
in this department of mining. ' i> •«.
A few instances of transport by boats may still be met with. BoMt
The boats used in the underground canal at Klausthal are 31 feat
' Jahrlmch fir das Bn-g- und Biittemcesen I
avf das Jf"' isn't r- 50
% Kmigreicfie SacMCK
456
MINING
[v/INDIKO.
Wmduig.
long by 4 fett 6 inches wide, and 2 feet 11 inches deep, liach boat
cames 6 or 6 tons.
Where roads have a strone gradient, inclmea pianes are
employed, either self-acting if tne mineral has to be lowered, or
worked by stationary engines if the mineral has to be raised
(see Coal, vol. vi. p. 69).
9. Winding/, or Raising in the Shafts, with the Machinery
and Apparatus required. — In speaking of the transport by
underground roads, we mentioned that the mineral is occa-
sionally brought to the surface on the backs of men or boys.
In other cases daylight is reached by adit-levels provided
with railroads ; but in by far the greater number of mines it
is necessary to hoist the mineral, and often much rubbish,
up vertical or inclined pits generally known as shafts.
In beginning to sink a shaft from the surface, or in
sinking a winze, hand-power applied by a windlass is
sufficient. The broken rock at the bottom of the shaft is
shovelled into a wooden or iron bucket (kibble), which is
drawn up by a rope passing round the barrel of the wind-
lass. When a depth of 20 or 30 yards has been reached
it is more advantageous to introduce horse-power, and the
usual machine by which this power is applied, called a gin
or horse-whim, is a common sight in many metalliferous
districts. It consists of a vertical axis carrying a barrel
or drum 8 to 12 feet in diameter, round which is coiled
the rope, which after passing over a pulley hangs down the
shaft. The axis carries an iron pin at each end, the lower
one working in a stone and the upper one in a socket m
the span-beam or cross-bar of the supporting frame.
Under the barrel is a long driving beam to which a bovss
is harnessed, and, as will be readily understood, the kibble
is drawn up or lowered down as the horse walks round.
rt is most economical to have two kibbles, for then they
balance each other.
■Where steam and water-power are not available, a large
number of horses or mules are sometimes harnessed to
whims, and ore raised from depths of 200 fathoms. _ These,
however, are exceptional cases; and, especially since the
introduction of portable engines, the use of steam-power
even for comparatively small depths, such as 100 yards, is
daily increasing. In hilly districts water-power is generally
at hand, and huge reservoirs are frequently constructed for
storing the rainfall, and so affording an adequate and conr
slant supply. It may be utilized by water-wheels, turbines,
and water-pressure engines.
There are three systems of winding by steam or water-
power which are in regular use :— (1) by buckets (kibbles),
baskets, or bags swinging loose in the shafts ; (2) by boxes
•working between guides (skips, Cornwall); (3) by cages
carrying one or more waggons.
Tlie buckets are made of wood, sheet-iron, or sheet-steel. Their
' shape varies ; it may be round or elliptical, straight m the side
or bulging in the middle. Fig. 84 represents a
kibble made of sheet-iron. When the shaft is
inclined, the side upon which the kibble slides
is carefully lined witti boards (Icd-planks) resting
■upon cross sleepers. Planks of hard ivood like
beech last longer and require fewer repairs than
deal boards, in the Harz, poles fixed lengthwise
take the place of boards, which are customary in
Great Britain. Even where shafts are perpen-
dicular a lining of planks is often put in round
the winding compartment, unless the space is
considerable, and the kibble then glides up
smoothly, and there is less risk of accidents. A
more modern system is to use wive-ropo guides
for the kibble, which is thus kept from swinging
about. Another ndvantiigo of this plan is that , f , ,u„
a licht catre can easilv be substituted for the kibble and used for the
ascentaml descent of the men. Mr Galloway has patented a method
of Binkinc shafts with wire-rope guides, the upper ends of which are
coiled upon drums at the surface. By adopting' this oxiK-dient tlio
Buides can be lengthened as the shaft is deepened.
A word must be e.aid about the actual loading and emptying of
the kibble. Sometimes, as already mentioned, the kibble is ill.-d
at the working place or from a shoot (/ja-a, Cornwall) carried down
into the level, and then conveyed on a troUey to the shaft, where
it is hooked on to the rope and drawn up. More frequently the
filler standing in the plui loads the kibble with a shovel ; and in
order to save time two kibbles are often provided, one being iilled
while the other is making the journey to and from the surface. ^"
this case it is necessary to have some kind of clevis, which will
enable the kibble to be readily detached from the winding-rope, and
quickly and securely fastened on again. On its arriving at the surfaco
the lander seizes an eye or ring at the bottom of the kibble by a
pair of tongs suspended by a chain, and the rope is now lowered. The
kibble is thus turned over and the contents fall into a tram -waggon.
The inconveniences of this method of winding are considerable,
especially in inclined shafts where the direction and amount oii
the inclination are not constant. There is great" wear and tear of
the bed-plank and casing-boards ; and, unless constant attention
is paid to repairs, places are worn out where the kibble catches,
cahsing the rope to break. The fall of a kibble and its contents
not only does much damage to the shaft, but also is a source of
danger to the men. The introduction of boxes {skips) working Skipi.
between guides or conductors was therefore a decided step in
advance, for the system allows the winding to be carried on with
less friction and with greater rapidity and safety. The guides are
often made of pieces of timber (like r, fig. 53) bolted to the end-
pieces and Jividings. It is only in perpendicular shafts that guides
made of wire-rope or iron rods can be applied. The skip is a box
of rectangular section made of sheet-iron or sheet-steel, with a
sloping bottom, and provided with a hinged door closed by a bolt for
discharging its contents. Fig. 86 ' shows how the skip rune upon
Fig. 84.
the guides by means of four cast-iron or (better) cast -steel wheels.
In an inclined shaft the guides sometiuies have iron rails laid on
them so as to diminish the wear. Some of the skips in Cornwall
are made to hold as much as a ton and a half of tiu-bearing rock.
The skip is filled with a shovel by a man standing in the plat, but
a better plan is to arrange shoots leading from largo hoppers, so
that the ore can be made to run in without any shoveUing. The
skip is sometimes tilted completely over instead of being emptied
bv a hinged door ; this arrongement is in use m some of the German
mines, where the skip is made of wood, and is guided on each side
bv two pins or rollers running between two conductors. W hen
the «kip has reached the surfaco t»o catches arc mude to support
the low'er rollers, whilst the upper ones pass through openings in
the front guides, and the skip, turning upon the lower ones, 18
tipped over and so emptied. ,. . v .,,„.• r.,.
The most satisfactory system of winding is by cages ; there is (..ato.
less handling of the mineral, and the hoisting jirocceds at far greater
speed This system, which is almost universal lu collieries, is
employed also lor working deposits of other minerals, and, tuough
~M^i^iet, Annates dcs Mines, m: 0, vol. ii., 1862, plate vU.
DRAINAGE.]
MINING
457
i n Tein-mimog the skip and kibble still prerail in England, the
manAgers are beginning to recognize the advantages of tbe cage and
equip ^eir mines with more modern appliances than hare hitherto
been cnstomarr. The cagea used in the mines on the Comstock
lode are very light and simple in construction, as will be seen from
fig. 86. Thn cage in fact is a mere timber platform, 5 feet by 4,
Fio. 88. — Cage used in Comstock Lode.
resting on iron bars p, and supported by iron rods on each side.
It is provided with a sheet-iron bonnet to protect the men if they are
inside, and also with safety catches (, t, wnich come into play if the
rope breaks. The hand levers k, k at the ends of the cage rarse up
clocks which keep the car in iti place during the ascent or descent j
g, g are guides for the end oL the crossbar b ; c, bar working teeth
tft by levers; /, "ear" or "shoe" embracing the guide-rod in
shaft ; r, lifting bar ; 5, strong spring.
The most important details concerning the use of cages, ropes,
and other hoisting appliances such as pulleys, pulley-frames,
detacliing hooks, and winding engines, have already been set forth
in the article Coal, vol. vi. p. 74; and it is therefore needless
to repeat these particulars, especially as the art of winding mineral
cheaply, speedily, and safely has been carried to a far greater pitch
of perfection in collieries than in the majority of metal mines. It
is often convenient to fix winding engines underground for the
purpose of sinking shafts and winzes, and drive them by com-
pressed air brought down in pipes from the surface.
Koepc The Koepe system of winding, which appears to be viewed with
system, favotir on the Continent, consists in having what is practically an
endless rope with one large sheave over the shaft, in the place of
the two drums. There are two cages, and the rope below them
acts as a coimterbalance, so that the load is uniform throughout.
Blsn- fhe most novel hoisting apparatus is that of Jl. Blanchet (Coal, '
chefs Tol. vi. p. 76), which has now been regularly at work in the Hot-
method, tinguer -shaft at ^pinac in Franco for the last six years. M.
Blanchet's method consists in fixing in the shaft a large pipe in
which is arranged a piston ; from this is suspended a cage' carr^nng
waggons. By exhausting the air above the piston the load is
gradually forced up by the atmospheric pressure below it. The
Hottinguer shaft is 660 yards deep, and the pipe is B feet 3 inches
in diameter, made up of a succession of cylindei-s of sheet-iron
about -fz inch thick and 4 feet 4 inches high, joined by flanges and
holts. Tlie 485 rings composing the long pipe weigh altogether
418 statute tons. The cage has nine decks, and arrangements are
made for unloading throe at a time ; each waggon holds half a ton,
so that the total useful load is 4.^ tons. The speed of hoisting is
20 feet per second. If two hoisting pipss are connected the dead
weights may be made to balance each ether, and the power
required is simply that which is necessary to overcome the weight
of the useful load. All the men prefer the pnanmatic hoist to the
ordinary cage for descending and ascending the mine, and are
regularly lowered and raised by it The advantages claimed by M.
Blanchet for this system are— (1) the possibility of hoisting from
depths at which rope-winding would no longer be practicable ; (2)
getting rid of the costly ropes and dangers connected with rope-
winding ; (3) better utilization of the engiije power; (4) improve-
ment of the ventilation and diminution of the amount of firedamp.
10. Drainage. ^~T\iQ mineral having been raised to the
urface, the task of the miner might appear to be at an
end ; but this is not the case, for it is further necessary
that he should keep his mine free from water and foul
air. These two indispensable operations of draining and
ventilating frequently require special appliances which add
considerably to the g^ieral cost of mining.
In all cases where it is possible, endeavours should be Dralnao*.
made to keep the water out of a mine, so as to save the
expense of pumping it ; and the method of putting in a
Watertight lining {tubbing) in a shaft has been already
described (Coal, vol vi p. 62). When large streams of
water happen Uj be intersected by underground work-
ings, and threaten to overpower the available pumping
machinery, or when it is advisable to save the expense
of draining abandoned workings, the entry of this water
into the mine may often be prevented by stoppings,
called damsj constructed of timber or brickwork.
In spite of all precautions, the miner generally has to
contend with water which percolates into the workings.
Four methods of getting rid of this water are available,
viz., adits, siphons, winding machinery, and pumps.
An adit, day-level, or sough is a nearly horizontal tunnel Adits,
with one end opening at the surface, allowing the water to
drain away naturally. In hilly countries mines are often
worked entirely by adits, and even when a mine is deepened
below the drainage level the utility of the adit is still
threefold ; — it lessens the quantity of water which tends
to percolate into the lower workings ; it lessens the depths
to which the water has to be pumped ; and, by f umishiDg
a certain amount of fall, it enables water to be applied as
power. On account of these important advantages some
very long and costly adits have been driven for the purpose
of aiding the miners in certain metalliferous districts.
Thus in the Harz the Ernest Augustus adit ("Ernst August
StoUn") has been driven a distance of nearly 6§ miles into the Klaus-
thai district. The total length of the adit, including the branches,
is no loss than 14 miles. It intersects many of the lodes at a depth
of upwards of 400 yards fi-cm the surface. The total cost of thia
adit is estimated at £85,500.
Another long adit is the celebrated "Rothschouberger Stolln,"
which unwatcrs some of the most important mines at Freiberg in
Saxony. The length of the main or trunk adit is more than 8^ miles ;
the gradient of the greater part of it is only 1 "18 inch in 100 yards.
The branches of this adit among the mines arc more than 16 miles
in length, so that the total length of the main adit with its
branches amounts to nearly 25 miles. Slany of the mines are now
drained naturally to a depth of 250 to 300 yards. The cost of the
main tunnel was £359, 334, or nearly £24 per yard, but this includes
the cost ofei"ht shafts, heavy- exi>enses for pumping from these
shafts, the wallin^of the adit for % mile, and all general expenses.
The length of time occupied in driving this adit was thirty-three
years. The "Kaiser Josef 11. Erbstolln "_ in Hungary is another
remarkable mining tunnel, which was commenced in 1782, and com-
pleted in 1378 at a total cost of 4,599,000 florins. It is 10^ miles
in length, extending from the valley of the river Gran to "the
town of Scheninitz, where it intersects the lodes at«depths varying
from 300 to 600 yards according to the contour of the surface.
In Cornwall the Great County adit was driven for the purpose
of relieving the Gwennap mines of their water, and it was pushed on
nearly to Redruth. This adit differs frpm the great works under-
taken in Germany by the fact that it commences in the mining
district, and, though the length of all the drivages amounts to more
than 30 miles, the water from the most distant mine does not run
more than about 6 miles before reaching daylight. The average
depth is only 70 or SO yards from the surface. In fact this great
adit, though a work of great utility when the Gwennap distiict
was in a flourishing condition, is merely a network of comparatively
shallow drivages, often along the lodes themselves, among the
mines, and therefore for boldness of execution cannot for one
moment be compared to the great Schemnitz, Fi'eiberg, and
Klausthal drainage tunnels which have just been mentioned. The
Blackett iJevcl in Northumberland is an adit which has been
driven a distance of about 4f miles, and it will have to be extended
about 2 miles further before reaching Allcnheads. Its depth from
the surface at this place will be about 200 yards.
The main part of the Halkyn tunnel in Flintshire is 2 milea
1256 yards in length, and the branch driven out to Rhosesmor
mine intersected the vein at a distance of 809 yards, making
a total of about 3^ miles, TLs greatest denth fVom the sui'faca
is 230 yaiUs, and the avei-ago denth in Halkyn Mountain about
XYI. — 58
458
MINING
[deainage.
215 yards. The length and depth of this adit arc not remarkable;
but the great quantity of water discharged is a point of considerable
interest and importance. It is estimated that this adit is now
discharging 15 million gallons or 66,000 tons of water in twenty-
four hours, although the outflow is purely natural, for no mines
are pumping water into it. It is now easy to understand that
the Rhosesmor mine, though provided with powerful pumping
machinery, was unablo to cope with the springs it encountered.
In the United States the famous Sutro timnel is an adit of which
the main branch, 4 miles in length, reaches the great Comstock lode
in Nevada at a depth of 1700 feet. The total cost of this tunnel,
which was completed in nine years, is estimated to have been
$7,000,000. The quantity of water running out daily in 1S79 was
12,000 tons, at a temperature of 123° Fahr. at the mouth of the
tunnel. All this water must otherwise have been pumped to the
surface at a cost estimated at S3000 a day. The obstacles to
, progress were very great : not only was the heat extreme, but
swelling ground was encountered which snapped the strongest
timber. Thanks, however, to the untiring energy of Mr Adolph
Suti-o, the difficulties were at last successfully overcome, and this
great work will long remain as a monument to his foresight, skill,
and patient pertinacity.
The Atlantic-Pacific tunnel,' which was commenced in 1880, mil
pierce the heart of the Rocky MounUins under Grey's Peak,
Colorado. It is being driven from both sides of the watershed, and
will have a total length of 4J miles from end to end.
Siphcrs. Siphons have been used for unwatering workings in
special cases ; but of course they will not act unless the
barrier over which the water is raised is very decidedly less
than 33 feet.
Winding When workings cannot be drained by tunnels or siphons
machm- it is necessary to raise the water mechanically, either to
the surface or at all events to an adit through which it
can flowaway naturally. If the amount of water is not
too considerable, it is often convenient to use the winding
machinery and draw up the water in special buckets {loater-
barrels) or tanks. The bucket May be tilted over on reach-
ing the surface, or it may be emptied by a valve at the
bottom. This means of raising water is often adopted
while sinking shafts, when it may be desirable to wait till
the whole or a portion of the shaft is completed before
putting in the final pumping machinery.
Puiiips. The varieties of pumps used in mines are numerous. In
small sinkings hand-pumps, either direct-acting or rotary,
may be applied ; steam-jet pumps on the principle of the
_ Giffard injectors are also used ; and pulsometers, though
requiring a large expenditure of steam, have the advantages
of being quickly fixed, of occupying little space, and of
working^ with sandy or muddy water. They are capable,
therefore, of rendering great services in special cases.
When wc come to the definitive machinery erected in
large mines of considerable depth, we find that the pre-
vailing types of pumps are few. They may be classified
as follows :— (A) lifting- and force pumps worked by rods
m the .shaft actuated by wind, water, or steam power ; (B)
force-pumps at the bottom of the shaft worked by steam,
compressed air, or hydraulic pressure.
_ A. In describing tlie first method we have to consider the motive
power, the rods, and the actual pumps themselves.
W indnjiUs have the disadvantage, wdiich is often fatal, that the
po\yer is not constant. By erecting an auxiliary steam-engine,
which can be set to work if wind fads, this evil is overcome ; and
at the Mona mines in Anglcsea a windmill pumps up water from a
oeptli of 80 fathoms at the rate of upwards of 90 gallons per
minute As the site of tlie mine is breezy, there is wind enough to
work the null about one-half of the time.
_ Water-power was for a long period the principal agent employed
in diainmg mines, and it is still of the greatest utility in many
districts, reservoirs being constructed to collect and store the
rainfall. Some idea of the scale upon which these works are
conducted will bo gathered from the following figures relating to
the Harz mines. In 1868 there were " 6i.\tyseven reservoirs
S?IT,,'!?„^" ^^%^ "'■ ^"^ ^"'^^- ""'• liiving a storage capacity of
336,000,000 cubie feet."= The total length of the various Icats,
Mininrj and Scientific Press, San Francisco, 1882, vol. xlv. p. 241.
'Notes on tiio new Deep Adit in the Upper Harz Mines," by H.
BiMnam Hcport of the Miners' Association of Cornwall and Beam-
thtrc, 1868, p. 21.
races, and other water-courses, including the six principal adits, is
about 170 statute miles. The net power extracted is reckoned at 1870
horae-power, but less than one-fourth of this is used for pumping.
Water-power is applied to pumping machinery by water-wheels,
turbines, and rotary or non-rotary water-pressure engines. Except-
ing the case of the latter, the rotary motion has to be converted into a
reciprocating motion by a crank ; and furthermore with turbines the
speed must be reduced very considerably by intermediate gearing.
Overshot wheels are the commonest prime movers when pumps
are worked by water-power; water-wheels are frequently constructed
40 or 60 feet in diameter, aud at the Great Laxey mine, in the Isle
ot Man, one of the wheels is no less than 72 feet 6 inches in diameter
and 6 feet in the breast. The power is conveyed from the water-
wheel by a connecting rod to a bell-crank {bob) placed over the shaft ;
and when, owing to the contour of the ground, the wheel has to bo
placed at a distance, it is connected to the bob by the so-called /a<
ro(h, made of wood, bars of iron, or wire-rope, travelling backwards
and forwards, and supported by pulleys or oscillating upright beams.
\A ater-pressure engines have the advantage of beii^ able at once
to utilize any amount of fall, and those which are direct-actin" can
be applied immediately to the main rod of the pumps. °
Steam, however, is the power used j>ar excellence in draining
mines ; indeed the first applications of steam-power were made for
this purpose, and Watt's great inventions owed their birth to the
necessities of mines which could no longer be drained by the water-
power at their command.
■The principal iypo of engine is that known as the Cornish engine, ComisH
which is a single-acting condensing beam engine working ex- ennna
pansively. ^ Its mode of action may be briefly described as foBows. '
The steam is let in at the top of the cylinder and presses doi-n the
piston, which is connected with one end of a large beam, whilst
the main rod of the pumps is attached to the other. When the
piston has completed^ its course the equilibrium valve is opened
by a cataract, and, the pressure on both sides of the piston being
now equal, the weight of the pump rods, or rather the excess of
their weight over that of the counterbalances, causes them to drop
and force up the water fiom the mine by means of the plungers,
which will be described immediately. Double-acting rotary-
engines working the pumps by cranks may also be met witli.
The rod in the shaft, known as the main rod or spear rod, is
usually made of strong balks of timber butted together and con-
nected by strapping plates fastened by bolts. It serves to work
either lifting-pumps or force-pumps, or both.
1 ig bi Fig. SS.
The lifting pump, or iJramng lift (fig. 87),' consists of the w
bore, the clack-piece, the clack-seat piece, the working bi
ind-
barrel
' Wicheli and Letcher on "Cornish Mine Drainage," /'OT'/y-rAircf
Anxuttl JReport of the Roijal Cornicall Polytechnic Socielj/, p. 311,
TENTItATIOS.]
MINING
46»
Above tho H-p.eco ">"« t„^^^,,f y'^^' Zol but occasionally of
a S'th?S arc';t I'-t Uh of more tban .ere
box can oe euoi.v r Tiluneer compared with a
expansion and condensation. The plunger or ram iB eeneiaUy
fixed directly on to the piston, and works in the same line, con-
seauenflT the power is transmitted to the plunger with the least
possible loss. The water is fbrced up the shaft in one long column.
L<Tnes and pumps of this kind are easily kept in order; all thff
parts are readfiy accessible. The miner is able to dispense wiA the
LavT beam, the massive engine-house, the long main rod and its
connexions and bobs, the various cisterns and plungers, and instead
he has a compact and easUy supervised machine and a simple Ime
of- pipes taking up but little space in the shaft; the p^p can
therefore be erected and set to work very quickly, and this is a
matter of the utmost importance in emergencies. It is true that
these direct-acting steam-pumps, ^en when worked by a compound
encdne cause a greater consumption of coal than the Cornish engme;
but ai a set off, there is the economy m first cost, erection, and
repairs which has led to their adopHon more especially m colhenea.
The steam is generated by boilers underground, or is conveyed from
the surface in well-jacketed pipes. . i • _
If natural water-power is available water-pressure enrines working
the plunger directly are often employed, anf indeed such water-power
may be Seated artificiaUy for use in workings where steam-power .3
lectionable on account of the heat. There «>-?_°*f^f f^^™» ♦"?
for employing water for transmitting power ; where the length o.
the rols iTvfry great, and they have to be worked quickly, there is
aVreatiabili^ to breakages; in order to overcome these difficulties
at^he mines on the Comstock lode Mr Joseph Moore'uscs a steam-
en<nne at the surface to work an hydraulic accumulator and then
bv pipes conveys the water under pressure to hydrau ic engines
wording plungers. These are fixed at 2400 feet from the surface
box can be eS^'sc^Twel up VT *; packing wears; this is one -^^fj'^^^^,, t^trco^^^mSelt high, to the level of
^-reat 'eaaon of L superiority of the plunger compared with a and for^^ JJ^^Jr^Tte exhaust water is returned to the surface m
K!cy*s
engine*
»'"^^: rSSns orthi. system-relate more to the engines em
•X ?y?rndrortr^o?i;xe?rL'^:;meti^^^^^
£rk^?.^^K^^r^£"asXern"en^pfL*Co^^^
l^^n disne^es Wh thf ponderous beam, but it has the great
dUadvantegTof orstructing^he mouth of the shaft. The use oF t>vo
cvlindeS combined, as invented by Woolf. causes less strain upon
the maS rod and pimps (pit-work) and machinery generally, as the
initial velocitv of the piston is smaller and the engine starts with
less'erk The cylinders are placed side by side or one above the
"' KUv of Bonn, has constructed engines on the Woolf system with
Steai acHng on both sides of the pistons. He makes the excess of
the weSt of the rod over that of the counterbalances sufficient to
Vaise only half the weight of the water and to overcome the fnction ;
and then ill the descending stroke the steam acts on the top of the
pKton and so makes up for^the insufficiency in force of the rods As
the steam acts on both sides of the piston the same amount is con-
sumed it is true, but a smaller cylinder will do the work, and tho
or^nal it of the engine is lessened. The same engineer of late
vears has put up several pumping engines in Belpum, Germany, and
fiance of 30 to 560 horse'-power, with a fly-wheel which serves su.nply
to reflate the stroke of the piston, so that the crank a ways stops
beforfor after the dead point tiU the cataract starts another stroke^
The engines are double-acting, ^vith two cylinders and beam The
advantlge of working with the fly-wheel is that the mam rod and
pumps are set in motion without the injunous jerk unavoidable
with a Cornish engine worked at a high rate of expansion.
.»-• .. ■ M Guinotte the well-known Belgian engineer, also adopts a
*"?"'"' ' flv whee" and the engines he has erected at Mariemont and else-
"«'"' where are single-acting rotary engines with one cyUnder. The
pecXrity of tie fly-wheel is that he can weight it in any way he
?S"?nd he so overcomes the difficulty, which occurs in other
FotTry machines, of its being impossible to work them below a certam
speed. His object has been to make the speed slow at the heginnuig
and end of a stroke, so as to avoid the injunous shocks to the valves
and machinery generally from sudden starts and stoppages. In
order to make the main rod act by traction only and not compression,
which may be advisable mth iron rods, the plungers are sometunea
reversed ; whilst Kraft of Seraing has introduced the Rittingcr
pump, which consists of a hollow moving plunger yth a valve mside,
and a plunger case above it working over a hollow fixed plunger.
Bv this arrangement both the up and the down stroke of the
engine cause water to be forced up; and this pump is used with
a double-acting rotary engine. , , , •. <■„„„
B We must now speak of the second class of pumps, viz., lorce-
pumps worked by steam, water-power, or compressed air at the
bottom of the shaft. « u ^ *i,««
The steam pumps are of very various descriptions,' but they
mostly consist of one or two plungers, or rams, set m motion by a
■ rotary or a non-rotary engine, which may or may not work with
~ 1 Michel! and Letcher on " Cornish Mine Drainage," Forty-Third
nrnuil Report of the Royal Cornwall Polytechnic Socxety, p. 211.
» Stephen Michell, Mine DTainaye, London, 1881.
the Sutoo tunneh" The exhaust water is returned to the surface ia
pipesand used over again. The pumps are now raismg 1600 to
^Th?r^™L7re-d':ii- is being -PpHed to a min^for drUUng
-tr^f KS ^U'p^^iucrr^^^^^^^
Seam for the drainagf oLm^U temporary sinkings ; and occas.on-
ally Targe pumps raising considerable quantities of water are worked
" this way
11 rendlation and Lighting.— The composition of the
air of the atmosphere is about one-fifth by volume of
oxygen and four-fifths of nitrogen, with a httle carbonic
acid gas ; more exactly, the standard amount of oxygen
may be taken at 20-9 per cent., and that of the carbonic
acid gas at 003 per cent. The atmosphere of mines is
subject to various deteriorating influences : not only do
nonous gases escape from the rocks into the underground
excavations, but also the very agents employed in the
execution of the work itself pollute the air considerably.
The dangerous emanations of fire-damirtn collieries have l'elet«..
been already described (Coal, vol. vi. p. 72) ; and ^ith <» ■ >- •
reference to this gas it is simply necessary to say that its
presence is not entirely confined to coal mines. Large
quantities have been observed in Silver Islet mine,« Lake
Superior, where several explosions have occurred, whilst
smaU quantities are met with in the stratified ironstone of
Cleveland, and also in the Cheshire salt mmes ; jets of the
eas may be seen constantly burning in the salt mine at
Bex in Switzerland; a Httle has been noticed also m lead
mines in Wales and Derbyshire. In the Sicilian mines the
amount given ofi by the black carbonaceous shales mter-
stratified with the sulphur beds is sufficient to cause
dangerous explosions. It has been pointed out (vol. vi. p.
72) that carbonic acid gas exudes from coalj^ it escapes
also from some mineral veins. At the lead mines of
Pontgibaud in central France it is so abundant that special
fans have to be provided for getting rid of it ; very distinct
issues of this gas may be observed at the Foxdale mines m
the Isle of Man, and in the Alston Moor district it is not
» Trans. Inst. Engineers and Shipbuilders in Scotland, 188?
• Engineering and Mining Journal, voh xmv. p. "?f
» A.Schondorff, " Untersuchung der ausz.ehenden Wetterstrome in
den Steinkohlenbergwerken des Saarbeckens," if'f'f/XxWvli'-
Millie. unnSalinen-Wesenim Pmissischm Staate, vol. XJtii. p. '»►
Sid a WtoklTr ''Die chemische Untersuchung derbei verscbiedenea
SeiSiUe^gnib n Sachsens ausziehendeu Wettersticme und ^
Erg^aisse," Jahrbuch fur das Berg- und mttqixoescn m KmgTa^
Sacluen au/das Jahr 1882, p. 65.
460
M i ^ i ^ G
uncommon. This gas is likewise given off in the Sicilian I
sulphm- mines, where also the highly poisonous sulphuretted
hydrogen is of frequent occurrence, the water in the work-
ings being often saturated with it. )SmaU quantities of |
mercurial vapour occur iu quicksilver mines.
;^tw!ni,ts Such then are the principal gases which naturally pollute I
ofrespi- {.jie atmosphere of mines, and have to be swept out by j
'f'''^' ventilation. In addition to these we have the products
^ ^' of the respiration of the men and animals in the pit, and
those due to the combustion of candles or lamps, and the
explosion of gunpowder, dynamite, (to.
Dr Angus Smith' reckous that two men wonting eight hoars,
and using 4 tb of candles and 1 i oz. of gunpowder, produce 25-392
cubic feet of carbonic acid (anhydride) at 70" F., — viz., 10'32 by
breathing, 12-276 by candles, and a-796 by gunpowder.
The products of the o.^plosion of gunpowder have been carefully
fitudied by Captain Noble and Sir Frederick Abel, and the follow-
ing figures, snowing proportions by weight, are copied from the
-raluable paper' containing the results of some of their researches: —
Total solid products
Total gaseous products..
Water
The solid residue of the mining powder consisted mainly of
potassium carbonate, potassium monosulphido, and sulphur. The
percentage -composition by volume of the gas produced was : —
Cai-bonlc anhydride
Cart)ODlc oxide.
Nitrogen
Sulphuretted hydrogen..
Harsh gas
Hydrogen
7 a
at -46
2-03
The volume (calculated for a temperatm-c of 0° C. and barometer
560 mm. of mercury) of permanent gases generated by the explosion
of 1 gramme of dry pow-der is —
Ciiitls Jb Harvey, No. 6 241-0 cutic centimetres.
Mining 300-3 „
ilM. Sarrau and Vieille have communicated to the Academy of
Sciences' the results of their researches concerning the decomposi-
tion of certain explosives, and more particularly gun-cotton and
nitrated gun-cotton. The follon-ing table shows, in litres, the
volume (at 0° C. and 760 mm. of mercury) of each of the gases per
liilogramme of the substance exploded in a closed vessel: —
Kind of Explosive
co.|co,.| n.
N. 0.
C.H,.
HS.| Total. 1
Pnve gun-cotton
Gun-cotton and nlu-ate of)
potash (50 per cent, of |-
Gun-cotton (40 per ccnt.U
234
...
"c'i
234
171
181
295
150
lC(i
"4
107
109
2U
147
65
45
6
25
4
17
T41
325
401
467
304
Nitroglycerin
Ordinary tjlasting powder
If, however, the explosive is decomposed ^t a pressure approach-
ing that of the atinospliei-e, the volumes (again at 0° C. and 760 mm.
of mercury) are very different, as sliown below: —
Kind o( Enplosivc.
Pure gun-cotton
Gun-cotton and nitrate of >
potaati (50 per cent, of each) (
Oun-coiton (40 per cent. land)
nitrate of ammonia (CO per V
ccnt.) j
Nltro-giyccrin
[VE-NTILATIOM.
oxide and carbonic oxide, and the analyses of MM. Sarrau and
Vieille confirm the practical experience of miners, who complain
gi-eatlyof noxious fumes when, owing perhaps to a bad detonator, a
charge of dynamite or tonite fails to explode properly.
The air of mines is finally deteriorated by organic matter con-
tained in the exhalations of the men and animals employed and
in the products of decaying timber, by dust, and by the solid par-
ticles constituting the smnke of explosives. It must be recollected
also that the injury to the air is not confined to the addition of the
gases and substances just mentioned ; but the proportion of oxygen
is diminished by the combustion of candles, by respiration, tha
decay of timber, and decomposition of some minerals such as iron
pyrites. Dr Angus Smith* sums up the rasults of his analyses of
the air of British metal-mines as follows : —
Percentage hy TOltim?.
Oxygen, average of 339 specimens 20-20
„ of ends 20-18
,, other parts 20-33
VVTien explosives are decomposed in this way they liberate nitric
' Report of the Commissimiers Appointed to Inquire into tfie Condi-
lion of all Mines in Grtai Britain to u-hich the Provisions of the Act
23 <fc 24 Vict. c. 151 do not apply. Appendix B., p. 221.
- "On Fired Gunpotvder," Captain Noble aud Mr F. A. Abel,
Phil. Trans., 1880, p. 278.
3 " Rechcrchcs cxpinmentales fiur la di^coniposition do quelques
cxplosifs en vase clos ; composition dea gaz formes," Comptcs JieJittus,
1880, pp.lOES and 1112.
Carbonic acid _ 0-785
Ho considers airwith 20 '9 per cent, oxygen as normal, and air with
proportions between that and 20-6 as impure, and where the per-
centage of oxygen descends below 20-6 he calls the air exceedingly
bad. According to these standards, only 10-67 per cent, of tb«
samples showed the air to be normal or nearly so ; 24 69 per cent,
were decidedly impure; whilst 64-63 per cent, or nearly two-thirds
of the samples were exceedingly bad. The amount of oxygen in
one specimen was as low as 18-52 per cent , whilst the carbonic
acid often exceeded 1 per cent, aiid.iu several instances 2 per cent.
It is evident that tneuty years ago the vci^tilaticn of British
metal mines wa.s anything but satisfactory, aud even now there is
room for improvement.
Having explained the reasons why the air of mines must
be constantly renewed, wi must now point out how this
desirable end is effected.
Two systems are employed, — natural ventilation and Systemi
artificial ventilation ; but, as both systems have been "' veiiti-
described (Coal, vol. vi. p. 70), little remains to be said '*'"'°-
here, especially as the ventilating machines in metalliferous
mines generally cannot for one moment be compared with
the powerful appliances employed in collieries. In vein-
mining there are generally many more shafts than in
collieries, and natural currents are set up which are often
considered sufficient for ventilating the mines ; never-
theless, the advanced workings, .such as the eniJs, rises,
and winzes, — in fact all workings in the form of a cul-de-
sac, — are likely to require special means ot ventilation
as soon as they proceed a little distance from the main
air-current.
The means of ventilating a drift or heading are various.
If a natural or artificial draught
exists at the mouth of the drift,
it may be diverted by an up- ,
right partition {brattice), or an . i
air-way may be constructed |.^
along the roof or floor by a
horizontal partition of planks
(air-sollar) (fig. 89). In this way a suflicient supply ia
secured at the end or fore-breast.
The water -blast is another simple appliance ; it is pre-
cisely the same as the
well-known tromiJ, and i . -«
it blows a current of air
through square pipes
made of boards, or
better through cylindri- 1.
cal pipes of sheet zinc.
The fall of water may bo apiji%a ly \\ .;;„„d„o ....Lti-j^t,
shown in fig. 90. The jet of water acts like an injector,
and creates a powerful current.
Small fans driven by boy.s, or better by small -water-
wheels or other machinery, arc frequently applied, and the
Fig. 89.
k
Op. cit., p. 222.
UGHTINO.]
MINING
161
Fig. 91.
LightiBg.
Harz blower (dvxk machine, Cornwall) (fig. 01) is not
uncommoo. This is merely an air-pump of very simple
construction -which is worked by the
main rod of the pumps, and can be
arranged so as to exhaiist the foul
air or force in fresh air
In working in blasting ground,
boring-machines driven by com-
pressed air are becoming more and
more largely used every day, and
the exhaust air escaping from the
machines is invaluable for ventilation.
At the same time, on account of
volley firing, the quantities of dele-
terious gases generated in a short
space of time are very considerable ;
and, in order to get rid of them
speedily, the compressed air may be
ipirators/ utilized for working a Korting aspirator or the somewhat
similar ventilator of Mr Teague, a jet of compressed air
turned into a ventilating pipe, which creates an exhaust
(tig. 92'). Naturally this .
ventilator is merely i
brought into play at the
time of blasting, and
while the boring ma- =^^=^
chinery is out of use. t
When compressed air is F-i
being supplied on a large scale to a mine for boiing and
winding machinery, it is often convenient to convey it by
a small gas-pipe to working places in which the ventilation
is inadequate. Of course, in one sense, it is very unecono-
mical to compress air to a pressure of 60 or 70 tt) to the
square inch for ventilating purposes only ; but, where com-
pressing machinery is always at work on the mine, it may
be better to be a little wasteful of cheap power at the sur-
face than to go to the greater expense of having a man or
boy to work a fan underground.
Mines are lighted by lamps, torctes, candles, and
electricity. The subject of safety lamps for fiery mines
has already been discussed (see Coal, vol. vi. p. 72), and
consequently the question of illuminating mines may be
treated in a very summary manner.
Lamps vary very much in shape and si^e. Tlie Sicilian miner has
B mere sL allow cup of unglazed pottery ; the Saxon a small tin or
brass lamp in a wooden box lined v.'ith tinplate
and open in front. In the Harz the miner prefers
a heavy flat iron lamp with a hook by which it is
stuck into the timber or any crack in the rocks ;
in France, northern Italy, and parts of Spain, the
iron lamp is lenticular in shape and also suspended
by a hook. In Scotland, and parts of Germany
and the United States, a small tin lamp of the
Shape shown in fig. 93 is very common ; tlie hook
enables it to be carried on the hat while climbing *^'S- *■'•
ladders, and to be fixed up underground. Olive oil and rape oil are
burnt in these lamps ; petroleum lamps are employed occasionally.
The miners of England and Wales still cling to the tallow candle;
and when surrounded by a lump of clay it can easily and quickly be
fixed in the working place or carried upon the hat when climbing.
Gas brought down from the surface answers for illuminating large
excavations, such as on-setting places and engine-rooms.
Up to the present time the electric light has been but little used
■underground on account of its want of portability, and the small-
ijcss of the spaces requiring illumination. Very often a few men
only are employed in each working place, and consequently the
expense incurred in fixing and shifting the lamps and maintaining
them aUght would be out of proportion to the value of the work
executed. However, an incandescent electric lamp has been invented
weighing only 10 lb, which gives the light of three candles for six
hours, and it may be reasonably expected that improvements will
be made which will render ^he electric light more available for
underground purposes than it is at present. When the area reqmr-
ing illumination is large, an arc-lamp may be used with advantage.
' Tram. Roy. Oeol. Soe. Cornwall, vol. x. n. 142.
.among the first successful applications of electric lighting to
underground excavations may be mentioned that of II. Blavier at
the Angers slate quarries.^ In the year 1879 he fixed two Serrin
lamps in one of the large underground chambers with an area or
2400 square yards, and he found that they gave light enough for aU
the men at work. The total cost, reckoning everything, viz., coal,
carbons, repairs, labour, depreciation of plant, and interest on capital^
is 50 francs per day ; the gas formerly in use cost 54 francs a day
and gave much less light. It is evident, however, that the arc lights
can only be applied with advantage in special cases where a large
number of men are concentrated in one working area which can Be
illuminated from one or two points.
The large chambers in the salt mine of Maros-Ujvar in Hungary
have been regularly Ughted up by electricity since 1880. The cost
is somewhat greater than that of the tallow, oil, or petroleum
formerly in use ; but, on the other hand, the illumination is better,
the men can do more work and are more easily superviseJ, whilst
the air of the mine is not deteriorated by the products of combustioD
of the lamps.^
12. Means of Descending inio and Ascending /rojn Hbib» ur
Mines. — Where mines are worked by adit-lewLs the men ac««-
naturaUy walk in along the ordinary roadjvays; such
miues, however, are exceptional, and the men generally
have to climb down and up by ladders, or are raised and
lowered by machinery. The means of access to and from
workings may be clas.sified as follows: — (1) steps and
slides ; (2) ladders ; (3) cages ; (4) man-engines.
If a lode or seam is iucUned at an angle or 40° or 50° from the Stepe^
horizon, steps may be cut in the floors of the deposit if it is firm
enough, or wooden stairs may be put in with a hand-rail. Even
vdth higher dips steps may be arranged by directing them in a Una
intermediate between the dip and the strike. In speaking of con-
veyance underground, reference has already been made to the practice
of carrying sulphur ore in Sicily and slate in Germany up to the ■
surface by steps ; and steps may be found in other foreign mines
and occasionally in Great Britain. They are much less fatiguing
than ladders placed so flat that part of the weight of the body rests
upon the arms. In some of the Austrian salt mines the men SU<5e»t
descend by wooden slides inchned at angles vaiying from 30° to 50°,
flattening at the bottom to destroy the velocity gradually ; the
ascent is elTected by steps.
Ladders are -eery largeiy usea in metal mines all over Ladders-.
the world, but they vary a good deal in different countries.
The ladder con.'iists of two sides and a series of rungs
{staves, Cornwall). The sides are usually made of wood,
and the rungs of wood or iron. The distance between the
rungs is important ; 10 inches from centre to centre is
sufficient, for climbing upon ladders with the rungs 12
inches apart is decidedly more fatiguing. On the Continent
wooden rungs are commoner than iron ones, and oak is
preferred. Sometimes the wooden staves, instead of being
round, are flat, so as to stand more wear, and iron sides
may be seen in places where dry rot is very bad. Platforms
should be fixed at short intervals, not exceeding 3 or 4
fathoms in perpendicular shafts, so
as to prevent falls from having fatal
consequences.
In many cases sufficient attention
is not paid to the angle of inclination
of the ladders. A ladder is climbed
with the least fatigue when the person
uses his arms simply to steady him-
self, and is not compelled to pull
himself up by them, as on a vertical
ladder, or to support much of the
weight of his body by them, as
happens with a very flat one. The
best angle is about 20° from the '
vertical, and in Belgium the autho- ^'S- ^*-
ritiea have very wisely decreed that no ladder shall be
inclined at an angle of less that 10° from the verticaL
Furthermore, of the two arrangements shown in fig. 94
T ' M. Blavier, "L'Eclairage ilectrique aux Ardois'e'^'s d' Angers,"
Annales des Mines, ser. 7, vol. ivii., 1880, p. 5.
' OaUmichischt Zdlschrifl fur Berg- und FiMeivjxst^, 1882, No.
25, p. 296.
462
M I IS I K a
[mkans op access.
A is better than B, because it not only affords a greater
inclination for the ladders, but also renders it less likely
that a man will drop through the opening (manhole) in
the platform (soUar) li he loses his hold and falls. These
may seem trifling matters ; but, leaving aside the question
of safety, the economy derived from fixing the ladders
at the best inclination Is by no means small. To make
this apparent we must recollect the depths to and from
which men have to climb, viz., 300, 400, and even 500
yards. It is important, therefore, to save every unnecessary
expenditure of energy, which, though trifling for one ladder,
becomes considerable when repeated a great number of
times. 'When a mine has reached a depth of 200 yards,
and a fortiori when it exceeds it, mechanical appliances
should be introduced for raising and lowering the men,
because time and strength are wasted by climbing.
Medical men also are agreed that excessive ladder-climbing
is injurious to the health of the miner. Therefore, both
upon hygienic and financial grounds, one of the first
thoughts in working a mine should be the conveyance of
the men up and down the shafts by machinery with the
'east possible fatigue.
tSiEes. In collieries and other mines worked by perpendicular
shafts, it has long been customary to raise and lower the
men by the ordinary winding machinery already described.
In the United Kingdom it is necessary that guides should
be used if the shaft exceeds 50 yards in depth ; safety-
catches and disengaging hooks (Coal, vol. vi. p. 75) are
.frequently applied for the purpose of preventing accidents.
The simplicity of this method of ingress and egress
uaturally renders it popular, and statistics prove that,
where proper precautions are used, it is exceedingly safe.
Mar- The first man-engine was put up in the Harz in 1833, and
Tfng'.w-. nine years later a similar machine was fixed in Tresaveau
mine in Cornwall. Since that time this very useful means
of conveying workmen up and down shafts has been resorted
to in other mining districts, and especially in Belgium and
Westphalia.
Two kinds of man-engine are in use, the double-rod machine and
the single-rod machine. The double-rod or original man-engine
•consists of two reciprocating rods like the main rods of pumps, carry-
ing small platforms upon which the men stand. The stroke is from
4 to 16 feet, and the little platforms are so arranged that the}' are
always opposite each otlier at the beginning and end'of each stroke.
Figs. 95 and 96 represent the rods in the two final positions. A
man who wishes to descend steps upon platform b (fig. 95) ; the rod
B goes down, and A goes up, so that b (fig. 96) is brought opposite
c. The man steps across from b to c, and then the rod A makes a
down-stroke, B an up-stroke. Platform c is now oppo-
site d (fig. S5), and the man again steps across ; and
thus, by constantly stepping from the rod as it com-
pletes its do\\'n-stroke, the man is A
gi-adually convoyed to the bottom of H
the shaft. By reversing the process, * b
■or, in other words, by stepping olf ^^l^Jl^j
on to the opposite platform as soon
as the rod has completed its up-
stroke, the man is raised to the sur-
face, without any fatigue beyond that
■of the very slight ellbrt of stepping
.sideways. If each rod makes four
up and down strokes of 10 feet each
per minute, the rate of ascent or
■descent will be 80 feet per minute.
Tiie single-rod man-engine has one
rod carrying steps, whilst fixed plat-
forms are arranged in the shaft so as «.-.. :,
to correspond exactly with them 0 L
<lig. 97). If a man wants to go
down, he steps on to A when the
np stroke is completed; the rod goes pj_ jg
down and A is brought down oppo-
/I
if^)"-
iito to the fixed platform 6, on to which he stem ofT.
1 h until the rod has finished its up-stioke. B
fig. 97.
He then
vaits on h until the rod has finished its up-stioke. U is hroaght
opposite h ; ho step3 on to B, the rod goes down and lie is brought
opposite c, wlierc ne steps off again and waits. By reversing the
oj)eration bo is gradually lifted to tho top of the shaft. Tliesini^le-
rod engine may be used by men f;oing ud whilo others are going
down, provided that there is sufficient room upon the fixed plat-
forms {soUars). The best plan is to have sollars right and left, as
shown in the figure, and then the ascending men step off to the left,
for instance, while tlic descending men take the right-hand eollars.
The ascending man steps on to the man-engine as soon as the
descending man steps off, and so the rod may be always carrpng
men up or down. The usual stroke in Cornwall is 12 feet, ana
there arc from three to livo or six strokes a minute. With five
strokes tho men d'iscend 10 fathoms a minute, or in other words a
descent or ascent of 300 fathoms occupies half an hour. Tho
reciprocating motion is best obtained from a crank, because in this
case tlio speed is diminished gradually at the dead points, and
the danger of an accident in stepping off and on is thereby dimin-
ished; mau-enginc'S, however, are sometimes driven by direct-acting
engines.
Wan-engine rods are constructed of wood or iron ; and at An-
dreasberg in the Harz each rod is replaced by two wire ropes. Like
a pump rod the man-engine rod requires proper balance bobs and
catches, and for the safety of the men a handle is provided at a
convenient height above each step.
The man-engine has one great advantage over the cage, which
consists in the fact that it can be safely applied in inclined and even '
crooked shafts ; and it is for this reason that man-engines have been
adopted in many metal mines unprovided with vertical shafts.
Careful comparisons as regards safety of travelling have been made
in Prussia between ladders, man -engines, and cages. The average
accidental death-rate is 3ho^vn by the accompanying table, which
gives averages for a period of ten years, 1871 to 1880: —
Ladders. Stan-engines. 1 Caeca.
Average antuml number of men travelling.
73,912
75
0-101
7,191 M,071
• 41 74
0-570 OllS
Average annual death rate oer 1000
B V
Tho table shows that the cage is nearly as safe as ladders. la
reality, if the actual distance travelled were taken into account, tho
cage would appear to be safer, because we may fairly assume that
the mines in which men are hoisted by cages are on the whole very
much deeper than those in which men ascend and descend by ladders.
The man-engine appears to be decidedly more dangerous than
either the cage or laddere. Here again a distinction requires to bo
made between the single rod and the double-rod machines, and tho
Prussian statistics include many of the latter. It will be readily
undei-stood that a fall in a naked shaft ■with few fixed platforms is
much more likely to be fatal than a fall in the shaft of a single-rod
man-engine which is closed with the exception of the manhole at
intervals of 12 feet. The Belgian warocquircs are rendered safer
than the Harz or Saxon man-engines by having a railing round the
back of each platform on the rod. Some of the double-rod machines
are made with large platforms so that two persons can stand ou
them, one going up and the other going down, or both travelling
in the same direction. The use of double-rod man-engines has been
entirely abandoned in the United Kingdom. The death-rate from
accidents on man-engines in Cornwall and Devon during tho
nine years 1873 to 1881 was C'lT per 1000 persons using them,
whilst the annual death-rate per 1000 persons using ladders
was slightly higher, viz., 0*19. If the actual distance travelled
were taken into account, the scale would turn more decidedly in
favour of the man-engine.
The cost of raising and lowering men by the man-engine is not
great. At Dolcoatli, a tin mine in Cornwall approaching 400
lathoms in depth (see figs. 6.2, 63), it is reckoned that Ud. per man
per day covers all expenses, including interest upon tho capital
expended and depreciation of plant.
■" 13. Dressing or Mechanical Preparation of Ores, — In a Dresang
largo number of cases the mineral, as it is raised from the °^ o*"^
jiune, is not ready for sale. It usually requires to be sub-
jtried to mechanical processes whereby the good ore is
'■iiLirely or partly freed from valueless veinstone. These
jTonesses, which in a few special instances are aided by
calcination in furnaces, are known as the dressing or
ineclianical preparation of the ores. As a rule the valuable
ore is specifically heavier than the veinstone, and most of
tlie separating processes are based upon the fact that the
hoavy i)article3 of ore will fall in water more quickly than
tho light particles of veinstone.
The processes of mechanical preparation may be classified
as follows :—(!) washing and hand-sorting ; (2) disintegra-
tion, or reduction in size ; (3) classification bv size or by
equivalence ; (4) concentration.
(1) Sometimes the ore coming from the mine requires Washinjj
simply to be freed from adliering particles of clay in order
DBESSUIO.]
MINING
463
Disin*
tegra-
tion.
Stone-
'breakc
to be rendered fit for sale, at other times the washing ia
necessary as a preliminary process previous to sorting by
hand. The operation is performed either by raking the
ore backwards and forwards upon a grating under a stream
of water, or in a box containing water, or, thirdly, by
means of an inclined revolving iron drum worked by hand
or any other motive power. " The machines used for this
purpose, known as washing trommels, are revolving
cylinders or truncated cones of sheet-iron provided with
teeth inside. The ore is fed in at one end, is subjected to
the action of a stream of water, and is diiicharged at the
other end.
The stuff, i.e., the mixed ore, veinstone, and country
rock, having been cleansed, it is now possible to make a
separation by hand. Women and children are generally
employed for this work, as their labour is cheaper and
their sight sharper than that of men. The stufi is spread
out on a table, and various classes are picked out according
to the nature of the products furnished by the mine.
Thus in a lead mine we may have — (a) clean galena, (6)
mixed ore, i.e., pieces consisting partly of galena and
partly of barren veinstone, (c) barren veinstone and country
rock. This is a most simple case; very frequently we
have to deal with a vein producing ores of two metals,
especially in the case of lead and. zinc, and then the
classification into various qualities becomes more com-
plicated.
(2) Reduction in size is necessary for two reasons. Even
when an ore is sufficiently clean for the smelter, the large
lumps are often crushed by the miner for the sake of
obtaining a fair sample of the whole, or supplying a
product which is at once fit for the furnace. The chief
reason, however, for disintegration lies in the fact that the
particiss of ore are generally found enclosed in or adhering
to particles of barren veinstone.
The disintegration is effected by hand or by machinery.
Large blocks of ore and veinstone are broken by men with
large sledge hammers, and the reduction in size is continued
very often by women with smaller hammers. Sometimes
the blow of the hammer is directed so as to separate the
good from the poorer parts, and hand-picking accompanies
this process, csJled cobhiru;. Ore may be crushed fine by
a flat-headed hammer (bucking iron) on an iron plate.
The machines used for reducing ores to smaller sizes are
very numerous ; here it is impossible to do more than
briefly call attention to those most commonly used. These
are stone-breakers, stamps, rolls, mills, and centrifugal
pulverizers.
The stone-breaker, or rock-breaker, is a machine with
two jaws, one of which is made to approach the other, and
l-'lo. 98. — Blake's Stonebreaker, improved by ilarsdea.
60 crack any stone which lies between them. The best-
known stone-breaker is the machine invented by Blake,
\Thich has rendered inestimable services to the miner for
the last twenty years, and the introduction of which con-
stituted a most important step in advance in the art of
ore-dressing. Its mode of action ia very simple. When
the shaft A (fig. 98) revolves, an excentric raises the
" pitman " B, and this, by means of the toggle-plates C, O,
causes the movable jaw D to approach the fixed jaw E
by about | inch at the bottoln. When the pitman descends
the jaw is drawn back by an india-rubber spring. The
jaws are usually fluted, the ridges of one jaw being
opposite the grooves of the other, and they are so con-
structed that the wearing parts are ouickly and easily
replaced.
Mr Marsden of Leeds has lately introduced a pulverizer,
constructed on the principle of the stone-breaker, which
will reduce large stones to the finest powder in one operas
tion. The moving jaw has an up-and-down as well as the
old backwards-and-forwards motion, and the stones are
first cracked and then ground by the double action.
Stamps are pestles and mortars worked by machinery, stamps.
The construction of the modem California stamp mill with
revolving heads is explained in Gold, vol. x. p. 747, and
the description need not be repeatei In Cornwall the
older form with rectangular heads still prevails.
It is impossible to give any correct average figures
representing the work done by a stamping mill, because
this varies with the hardness of the stuff treated and the
fineness to which it must be reduced. However, it is usual
in Cornwall to reckon 1 ton of tinstufi and in California 1
to 1;^ ton of gold ouartz stamped per horse-power in
twenty-four hours.
Stamps are principauy usea in dressing the ores of gold,
silver, and tin, but are occasionally employed for those of
copper and lead. The stamps described at vol. x. p. 747
act simply by gravity. Another form, which has met
with favour in the Lake Superior district, is the direct-
acting or Ball stamp, which works like a steam hammer,
the blow of the iead being assisted by the pressure of
steam. At the Calumet and Hecla Mill, Lake Superior,
each Ball stamp is capable of crushing 130 tons in twenty-
four hours. In a third kind of stamps, the heads are lifted
by a crank and the power of the up-stroke compresses a
cushion of air (pneumatic stamps) or a spring, storing up
power which m?.kes the dovra-stroke strike a heavier blow.
Revolving rolls were introduced in the west of England Rolls.
' in the early part of the present century to replace bvchinf/
by hand. The machine, now often known as the Cornish
crusher, consists of two cask-iron or steel cylinders which
revolve towards each other, whilst at the same time they
are kept pressed together by levers or springs. The
cylinders or rolls are generally from 18 inches to 2 feet or
2 feet 8 inches in diameter and 12 to 22 inches wide.
Stone mills construsted like flour mills are employed in Uills^
some countries for reducing ores to powder; and the
arrastra, which consists of heavy stones dragged round
upon a stone bed, has rendered good service in grinding
and amalgamating gold and silver ores, in spite of its being
slow and cumbersome. Edge-runners (Chilian miUs) also
deserve menfion.
Iron mills, known as jxtns, with grinding surfaces made
of chilled cast-iron and arranged so that they can be
quickly and easily replaced when worn out, are greatly in
vogue in the United States for the treatment of ores of
gold and silver ; the ore delivered to them is already finely
divided, ^nd they are intended, not only still further to
reduce the size of the particles, but also and more especially
to effect the amalgamation of the precious metals with
quicksilver. The pulverizers used in Cornwall for grinding
grains of tin ore with a little waste still adhering to them
are also iron mills
The centrifugal pulverizers are machines by which the
464
MINING
rsBEseui'o.
Oentri- pieces of ore are thrown with great velocity against bars or
•"sal arms, or against each other, and so reduced to powder ; in
pitlrer- Qj-jjgj. machines iron balls or iron rollers are whirled by
centrifugal force against an iron casing and grind any
mineral contained inside it. These pulverizers are much
less used than stone-breakers, stamps, and rolls for the dis-
integration of metallic ores.
Classifi- (S) Classification of a crushed ore into sizes is absolutely
cation of necessary in some cases and ad\'isable in others, because
""'• the subsequent concentration is dependent upon the fall
of the particles in water, as will be presently explained.
Classification by size is effected by sieves. Hand sieves
and flat sieves placed one above the other have been super-
seded at most dressing establishments by cylindrical or
conical revolving screens known as trommels. These
screens are made of wire web or of perforated sheets of
metal, and they are often arranged so as to discharge one
into the other, so that the ore from a crusher can quickly
be separated into classes of various sizes.
With sizes of less than 1 millimetre (Jj inch) trommels
are no longer employed, and recourse is had to the .so-called
separators or classifiers. These are boxes in the shape of
inverted cones or pyramids into which the finely crushed
ore is brought by means of a current of water ; a jet of
clean water is often made to rise up in the bottom ; the
larger and the specifically heavier particles fall and are
discharged vrlth a stream of water at or near the bottom,
whilst the smaller and specifically lighter particles flow
away at the top. The separators do not effect a true classi-
fication by size ; they merely caiise a division by equivalence,
a term which wiU be explained immediately.
Concen- (4) We now have to deal v/ith the enriching of the ore,
tiaUon. or the concentration of the valuable particles into as small
a bulk as is economically advantageous. The concentration
is generally brought about by the fall of the particles in
water. Occasionally the fall in air is utilized; mercury is
employed as a collecting agent in the case of gold and
silver, and in a few instances magnetism can be applied.
The concentration in water depends upon the difference
in specific gravity of the valuable ore and the waste vein-
stone or rock. A piece of galena with a specific gravity of
7 "5 sinks to the bottom more quickly than a similar piece
of quartz, the density of which is only 2 '6. Nevertheless
a large piece of quartz may fall to the bottom as quickly
as a small piece of galena. Particles which have equal
velocities of fall, though differing in size and specific
gravity, are said to be equal-faUing, or equivalent. P. von
Eittinger shows that a sphere of quartz of \ inch in
diameter would sink in water exactly as quickly as a sphere
of galena of -Jj inch in diameter, and these two particles
are therefore equal-falling. Consequently, before wa can
separate properly by water it is neoessary to classify the
particles by size, so that equivalence shall not prevent a
separation or lessen its sharpness. It is nevertheless true
that in the early part of the fall of equivalent grains the
influence of the specific gravity preponderates, and the
denser particles take the lead ; therefore, by a frequent
repetition of very small falls, particles which have not been
closely sized may still be separated.
JigEsra. Thu principal machine for concentrating particles of sizes
ranging between 1 inch and -^j; inch is the jig or jigger.
The hand jigger is merely a round sieve which is charged
with the crushed ore and then moved up and dowu in a
tub full of water. The particles gradually arrange them-
selves in layers, the heaviest on the bottom and the lightest
at the top. On lifting out the sieve the light waste can
be skimmed off with a scraper, leaving the concentrated pro-
duct below ready for the smelter or for further treatment.
Similar sieves worked by machinery were for a long time
employed in dressing establishments, but the introduction
of the improved continuous jiggers has led tcr the£
abandonment in all works of any importance. The cod
tinuous jigger is one of the
most useful dressing ma-
chines of the present day.
It consists of a box or hutch
divided by a partial partition
into two compartments ; in
one is fixed a flat sieve s (fig.
99), which carries the ore,
and in the other a piston p
is made to work up and
down by moans of an- ex-
centric. The hutch being
full of water, the movement
of the piston causes the water
to rise up and fall down
through the ore, lifting it
and letting it fall repeatedly.
The effect of these frequent
lifts and falls is tocause a sepa-
ration of the previously sized
Fig. 99.
ore into layers of rich mineral at the bottom, light waste at
the top, and particles of ore mixed with waste in the middle.
Tho great value of these jiggers is the continuous discharge of
the products without stoppages for their removah Several methods
are in vogue, viz., the end discharge, the central discharge, and
the discharge through the meshes of the sieve. With the first, the
enriched product lying at the bottom of the sieve passes out through
openings at the end of the jigger, and the amount escaping is
governed by an adjustable cap or shutter, by which the size of the
openings can be increased or diminished at pleasure ; the middle
product can be discharged by openings placed a httle higher up,
whilst the waste is washed over the top of the end of the jigger at
each pulsation. Very often a fh'st sieve simply separates a conceu-
trated product and discharges the poorer product into a second sieve,
where a similar separation is effected. With the central discharge,
a pipe is brought up through the bottom of the sieve, and the size
of the opening for the escape of the concentrated ore is regulated
by a cyUndrical cap
which can be raised or
lowered by a screw. Tho
discharge through tho
sieve is especially adapted
for the finer products
from the crusher, though
it is also used in some
cases for grains up to i
inch in diameter. The
mesh of the sieve is
chosen so that the par-
ticles imder treatment
will just pass through,
but above the sieve a
layer of clean ore is
placed which prevents
anything but the heavier
particles from being dis-
charged. The pulsations
of tlie water, as before,
cause a separation inlo
layers, and the heavy
rich particles lind their ^. ,.^
waytl.roughtbobednnd V^S■^^0.
drop into tho hutch, whence they can be drawn oft' through a hole
at pleasure. The poorer part passes over a siniple sill at the end of
the sieve, or to a second sieve if necessary. Three or four sieves
are occasionally arranged in a row in one machine.
Fig. 100 is a section through the two sieves of a Harz §and jig.
The pistons act in the manner explained by fig. 99.
The smaller sizes are concentrated by a variety of
machines. The action of many of them is based upon the
behaviour of particles carried down an inclined plane by a
thin stream of water. If the gradient of the plane and
tho strength of the thin current are properly arranged, the
denser particles will bo deposited and the specifically lighter
ones washed away, although they may be equal-falling if
allowed to settle in deep water.
xs^"^
■BESSIKC]
MINING
465
The principal machines for concentrating fine sands and
sEmes are the frame, rotating frame, percussion frame,
side-blow percussion frame, revolving belt and True
vanner, the hand huddle, the round buddle, and the keeve.
The frame is simply an inclined wooden table upon which a thin
deposit is formed by thp sLeet of ore-and-waste-bearing water whi'h
is made to flow over it gently. The stream is then stopped and i
deposit washed off by hand or automatically, and collected in i-
for subsequent retreatment by similar appliances if necessary.
The rotating frame is a round table with a very flat convex
eonical surface ; the ore for suspension flows on at one part of the
centre and forms a thin deposit which is richest at the top and
poorest at the bottom, and tnis deposit is washed ofl" so as to form
I two classes by means of jets of water, under which the table passes
as it turns round. Concave rotating tables, fed at the circumfer-
ence, are also employed.
The percussion frame, the Stossheerd of the Germans, is a table
enspenaed by four chains which receives a succession of blows
from a cam in the direction of the stream flowing over it ; after each
blow it bumps against a piece of timber before receiving the next
blow. These bumps cause the ore to settle, and after a thick
deposit is formed it is dug off with the shovel, the upper end
being richer than the middle or the tail.
Rittinger's side-blow percussion frame is a suspended rectangular
table ABCD (fig. 101), receiving blows and bumps on the side and
not on the end. A stream of orey s „
water S is fed on at the corner A;
clean water W is sup}>iied by the
other head-boards H, H, H ; and
the table is pushed out by cams in
the direction of the arrow, and is
driven back by a spring so that
the cross-piece E strikes against a
! bnmping-block K. The light par-
ticles travel down the table much
faster than the heavy ones, and
take a comparatively sti^aight
course ; whereas the heavy and
richer particles remain on the
table, eubiect to the influence of
the side-blows, for a much longer
time, and travelling alongacurved
path reach the bottom at F. The
uiiddle_ class is discharged at G
and the poor waste at K. The
exact degree of richness of the
products can be regulated by alter-
ing the pointei-s, strips of wood
which can be turned so as to divide the stream of ore and waste
where thought most desirable. The great advantage of this
machine over tut- old percussion frame is its continuous action.
The Frue vaiiiicr (fig. 102) may be looked upon as an improved form
of Brunton's simple revolving belt. It is an endless band of india-
rubber cloth, tianged on each
side, which i-cvolves slowly in ^^-<
tlie dii'cction of the arrows, ^^ —
whilst at the same time it is
shakcu sideways by a crank
motion. The orey water is fed
on at A, clean water at B. The
natural path of the particles is
dowu the inclined belt, but the specifically heavier ones settle upon
it and are carried upwards. Those that can resist the action of the
stream of clean water at B go over the end and are washed off as
the belt passes through the tank. The poor stufi' falls into the
waste launder. The degree of concentration can be regulated by the
slope and speed of the belt and the strength of the streams of ore
and water. The Frue vanner has the disadvantage that it makes
' ^nly two classes, rich and poor, without any intermediate product.
The hand buddle is a reetangiilar wooden box with a sloping
bottom. A stream of fine ore and waste suspended in water is fed
in at the upper end and giadually forms a deposit on the bed of the
buildle. A boy with a broom keeps the to]> of the sediment smooth,
so as to ensure regularity of action. After a thick deposit has
accumulated, it is dug out in sections which decrease iu richness
from the upper end {head) to the lower end (tail).
Kourid buddies, like rotating frames, are of two kinds, convex and
concave. Tlie convex round buddle (figs. 103 ' and 104) is a circular
pit wi til a truncated cone, or head, of varying size in the centre, and
a bottom sloping towards the circumference. The orey stream A
fallih" over this head runs do«-n gently, depositing the heaviest
particles near the top, the lighter ones further down, whilst the
Fig. 101.
Fig. 102.
lightest of all Bow away at C. The surface of the sediment is kept
even by revolving brushes D. _ This machine may he compared to
Fig. 103.
a number of hand buddies arranged radially round a centre. The
deposit that is formed is dug out in rings of varying richness.
> ' Henry T. Ferguson, " On the Mechanical Appliances Used for
Dressing Tin and Coi>per Oks in Cornwall,", Proc. Inst. Meeh. £na..
1873 pL 41.
Fig. 104.
The concave buddle ia a circular pit with the bottom slopuig to-
wards the centre. The stream of ore is fed all round the circum-!
ferenco, and runs inwards to the middle, where the lightest particles
escape. The rich head is of course near the circumference.
The keeve is a large tub in which the fine stuff is stirred with Kea»B
water and then is allowed to settle from a state of siispension
while blows are being struck on the side of the tub. The deposit
is afterwards scraped out in layers which increase in richness as
they approach the bottom.
The series of processes employed in dressing an ore varies, Drestim
not only according to the nature of the particular mineral different
to be concentrated, but also according to the size of its o™'-
particles and the nature of the other minerals with which
it is associated.
With gold the reduction in size ia usually effected by ooldj
stone-breakers and stamps, and much of the metal is then
caught by mercury j what escapes is concentrated with its
accompanying pyrites by inclined tables covered with
blankets, or by buddies, and the concentrate is treated by
amalgamation or chlorination. See Gold, vol, x. p. 746.
In the case of silver the ore is frequently pulverized by SiHei
stamps, and the resulting pulp amalgamated in pans or
barrels. The ore may also be concentrated by any of tho
various machines described, and delivered to the smelter.
Many of the ores of silver are sent to the smelting works
without any concentration by water, as this would cause a
serious loss.
Lead ore is generally crushed by rolls, often after a pre- Lead.
liminary reduction in size by the stone-breaker. The'
crushed ore is classified by revolving screens down to the
size of 1 mm., and the resulting grains concentrated by,
jigging; dredge, or grains of ore and matrix, must be
recrushed, sized, and jigged. The finer sizes are classified
by pyramidal boxes and concentrated by frames, rotating,
tables, and buddies.
Zinc ore is dres.sed in the same way as lead ore ; andj^as
galena and zinc-blende are frequently intimately associated
together, it is necessary to separate them by the use of ths
jig, buddle, and frame.
16—18
466
MINING
[LEaiSLATIOir.
Jla» Tin-bearing rock is crushed by the stone-breaker and
then stamped fine. The resulting sand and slime may be
concentrated by the repeated use of the round buddle, with
the keeve for a final cleaning ; but often the sand only is
enriched by the buddle, whilst the very finest particles,
constituting an almost impalpable mud (slime) when mixed
with water, are treated by frames. "When much pyrites
is present it is necessary to make a preliminary concentra-
tion and roast the enriched product (tvitts) in a furnace.
The calcination converts the heavy iron and arsenical
pjTites into a light oxide which can be got rid of with the
jrest of the waste by huddling and framing. The final
product from the keeve is clean enough to approach pui-e
cassiterito in the percentage of metal. Alluvial tin ore is
concentrated in sluice-boxes, and sometimes by jiggers, after
a preliminary treatment in a puddling-'machine (Gold,
vol. X. p. 7-15) if there are balls of clay which have to be
broken up. When the alluvial ore occurs as a hard con-
glomerate [cement), it has to be stamped.
Copp;..''' Copper ores arc treated by crushing by rolls and some-
times stamps, sizing by trommels, and then jigging and
huddling ; but, as .some of the ores are very friable and
easily carried av.-ay by water, hand-picking is employed
to a greater extent than with lead and tin ore, and the
enrichment by water is not carried so far on account
of the inevitable loss that would ensue. The amount
of concentration depends upon the distance from the
smelting works, and the mine-owner has to calculate
whether it is best to get a low price for a largo quantity
of ore, after paying the carriage, or a higher price for
a smaller lot [parcel) when due allowance has been
made for the cost of dressing and loss sustained in that
process. Thus, for instance, in Cornwall, the ore containing
copper pyrites is dressed so as to contain only from 5 to 8
or 9 per cent, of metal, because it can easily be conveyed
to Swansea by sea, and because further reduction in bulk
would cause greater loss in value than the saving of freight.
1,033 in The loss in dressing is very considerable. P. von
VlressiD,--. Rittinger estimates it at from 80 to SO per cent., and
stubborn facts bear out his conclusions. Heaps of refuse
from dressing floors are frequently worked over again with
profit; and in the year 18S1 no less than 909 tons of
" black tin " (i.e., concentrated tin ore fit for the smelter),
worth il35,283, were extracted from the muddy water
allowed to flow away from the dressing floors of some bf
the principal Cornish tin mines.
The fall in air lias been employed instead of the fall in water for
concentrating purposes, and several ingenious air-jigs have been
constructed and Tvorked upon tliis principle.
Separa- In exceptional cases magnetic attraction may be utilized. Mag-
tioE by netic iron can be separated in this way, and tlio magnetic process is
maniet- applied for treating mixed blende and chalybite, the specific gravities
isnf of which are too close to render concentration by water practicable.
The mixed ore is calcined, and the chalybite is thus converted into
magnetic iron, which can be extracted by a magnetic separator,
leaving saleable blende.
Recent Before concluding this part of the subject we \vill briefly
improve- enumerate the principal improvements that have been
'"*"'^- ' made in metal-mining during the last quarter of a century
They are as follows : — diamond-drill for prospecting ;
machine drills for driving, sinking, and stoping; use of
compressed air for winding underground ; stronger explo-
•sives, especially the nitro-glycerin compounds dynamite
and blasting gelatin; increased use of steel for various
purposes; Blake's stone-breaker and continuous jiggers;
•. xtended application of hydraulic raining ; larger employ-
ment of electricity both for blasting purposes and for
signalling by telegraph and telephone. It may be reason-
ably hoped that ere long electricity will render increased
.services to the miner for lighting the workings and for the
transmission of power.
14. Recent Lcjidalion afecllng Mine:: in the UrUled King- Rw.-nt
dom.^ — In England the person owning the surface of a free- Br.tist
hold is prima facie entitled to all the minerals underneath, l^^"*
excepting in the case of mines of gold and silver, which be- *
long to the crown. The €ro\vn, however, does not claim
gold and silver extracted from the ores of the baser metals.
The omiership of the minerals can be, and often is, severed
from tliat of the surface, the i3.tter being sold whilst the
mineral rights ai'e reserved by the original owner. Local
customs, now regulated by Acts of Parliament, are still in
force in Derbyshire (High Peak Mining Customs and
Mineral Courts Act, 1851, \i &, 15 Vict. c. 94, and the
Derbyshire Mining Customs and Mineral Courts Act, 18.") 2,
15 <& 16 Vict. c. 43) and in the Forest of Dean (1 i; 2
Vict. c. 43, and 24 & 25 Vict. c. 40). The Stannaries
Act (32 & 33 Vict. c. 19) regulates the commercial dealings
of mining companies in Cornwall and Devon, and provides
for their liquidation.
The working of mines in tno United Kingdom is con-
trolled by five Acts of Parliament, viz., " The Coal Mines
Regulation Act, 1872" (35 & 36 Vict. c. 76), "Tha
Metalliferous Mines Regulation Acts, 1872 and 1877" (35
& 36 Vict. c. 77, and 38 & 39 Vict c. 39), "The Stratified
Ironstone Mines (Gunpowder) Act, 1881 " (44 & 45 Victj
c. 26), and "The Slate Mines (Gunpowder) Act, 1883"^
(45 Victi c. 3). The last three Acts simply refer to tha
annual returns, and exemptions from certain restrictions
concerning the use of gunpowder.
The Coal Mines Regulation Act applies to mines of coal,. stratiSeS
ironstone^ shale, and tii-e-clay. The iMetalliferous Mines liegulation
Act applies to all mines not included under the Coal Slines Act,
and therefore controls not only workings for lead, tin, copper, and
iron, commonly known as mines, but also the salt-mines, and under-
ground quarries worked for stone, slate, or otlier earthy minerals.
The principal provisions of the Coal Mines Rcralatiou Act have
beeu set forth at vol. vi. p. 78 ; those of the lletalliferous Mines
Regulation Act arc similar, but less strict owing to the almost
complete absence of iire-damp. One important difference is that
the manager of a mine under the Metalliferous Act need not hold
E.ny certificate of competency or service.
Other Acts of Parliament are the "Explosives Act, 1875" (33
Vict. c. 17), regulating the manner in which explosives are stored ;
the "Elementary Education Acts, 1876 and 1S80" (38 & 39 Vict,
c. 79, and 43 & 44 Vict. c. 23), regulating the emploj-ment of
children ; tho " Factory and ^Vorkshop Act, 1878" (41 Vict. c. 16),
which applies to the diessins floors of mines under the Metalliferous
Mines Regulation Act.
The statute of Elizabeth (43 Eliz. c. 2) which was passed for
raising money for tho relief of tho poor mentions coal mines,
but omits other mines; these have been made subject to poor-
rates by "The Rating Act, 1874" (37 & 33 Vict. c. 54). Tho
"Employers' Liability Act,. 1880" (43 & 44 Vict. c. 42), extends
and regulates the liability of employers to make compensation for
personal injuries suifercd by workmen in their service. Fii.aUy,
if, as sometimes happens, works are put up at a mine for roasting
copper ores with common salt in order to extract tlio metal by tha
wet way, the provisions of tho "Alkali, kc. Works Reguktiou
Act, 1881" (44 & 45 Vict. c. 37), must be attended to.
It is thus very eviJeut that tho laws aflecting mines have received
most important additions during tlie last few years.
15. AccidenU in Mines. — Mining is one of the occupa- Accldartm
tions that -may decidedly be called hazardous. This fact
has been thoroughly impressed upon the public mind by
explosions of fire-damp in collieries ; but, though accidents
of this kind are appalling, owing to the number of victims
who perish at one time, fire-damp is by no means the worst
enemy with which tho miner has to contend. Falls of
roof and sides both in collieries and metal mines are far
more fatal in their results. With the risks attending
the colUer's calling we need not deal, as statistics upon
' For information concerning tho laws relating to mines in the United
Kingdom, see "W. Bainbridge, A Treatise m the Law of Mints and
Minerals, 1878, and .\rimael Rogers, Tlit Law relating to Miita,
Minerals, and Qtiarries in Orcat Britain and Ireland, with a Sun-
mary (/ tlie Lava qf Foreign Statta, 1876.
ACCIDENTS.]
MINING
467
this subject have been ab-eady given (see Coal, vol. vL I mines prove that the occupation of the metal mmer is
p. 79) ; but the figures below relating to metalliferous | very little leas dangerous.
Hints classed under the Metalli/crous ifina Regulation, Act in Oreai Britain and Ireland.
1
Nnmber of DeoUu from Accidents.
Death .rate from .Occidents per
1000 persons employed.
Onder Groond.
Above
Ground.
General
Total.
Under Gnmnd.
Above GnniAd.
TotaU
Falls of
Ground.
In
Shafts.
Mlscel-
laneocs.
Total.
Under
Groaod.
Above
Gronnd.
Under Groond
and
Above Groond.
1874
1875
1878
1877
1873
1879
1880
1881
1883
34,03«
34,905
34,109
34.095
80,624
38,S65
82,045
33,291
83,814
22,325
23,168
23,388
23,300
20,834
18,796
20,863
21,651
21,692
56,361
68,073
67,497
57,395
51.458
47,060
52,903
64,942
55,606
40
32
25
41
27
24
81
3S
30
34
35
16
21
19
18
21
22
27
16
33
23
24
23
16
19
32
17
89
lOO
64
86
69
56
71
90
74
14
19
6
11
8
8
13
9
18
103
119
70
97
77
64
84
99
93
2-61
2-86
1-87
3-52
2-25
1-98
2-21
2-70
2 18
0-62
0S2
0-26
0-47
0-38
0-42
062
0-41
083
1-82
205
1 21
1-69
1-49
1-36
1-59
ISO
1-64
Total and arenfres )
for tho nine years )
595,184
196,016
491,200
286
211
203
699
108
SOS
2-87
0-54
1«3
This table ' shows that tho average accidental mortality of the
persons employed underground in metalliferous mines is 2*37 per
1000. During the ten years 1873-1882 the corresponding mor-
tality at mines under the Coal illines Act was 2'57, showing a
diiference of only 0"20 per 1000 in favour of the metal miner ; and
when we take the well-known metalliferous tlistrict of Cornwall
and Devon we find a death-rate for the ten years mentioned of
2'63 per 1000, which therefore exceeds that of coal mines.
Reference to the table shows that more than one-third of the
deaths were caused by falls of ground. The accual percentages of
the deaths are as follows: — falls of gronnd 35 5, in shafts 26 2,
miscellaneous 25"1, on surface 13*1. The accidents in shafts are
due to falls from ladders, cages, and man-engines, ropes and chains
breaking, overwinding, and other causes, whilst the miscellaneous
accidents include numerous fatalities in connexion with blasting
operation!). The surface accidents aiB mostly caused by persons
becoming entangled in machinery, and there have been several fatal
boiler explosions.
f In spite, however, of all the dangers to which miners are exposed,
they are less likely to be the victims of accident than railway ser-
vants, among whom the rate of fatal accidents varies from 2 "5 per
1000 on pjissenger traffic lines to 3'5 per 1000 on lines possessuig
a heavy ^oods traffic'
Statistics concerning accidents in mines are published by many
foreign countries; the most minute are those prepared by the
Government mining engineers in Prussia. The average annual
death-rates per 1000 persons empljyed below ground and above
ground from accidents iii mines in Prussia during the fifteen years
1867 to 1881 have been: — coal mines 2952, lignite mines 2474,
metal mines 1-446, other mines 1-693, all the mines together2-476.
In making any comparison betw-een these figures and those we have
given for Great Britain, it is necessary to recollect that the mines
under the Coal Slines Act include some workings which in Pnissia
would be classed as metalliferous, and that British mines under
the Metalliferous Act include underground stone-quarries.
Before concluding the subject of accidents, it is necessary to
point out that successful efforts have been made of late years to
mitigate their results. In the first place, persons equipped with
the Fleuss breathing apparatus can now enter mines after explosions,
in SDite of the noxious and irrespirable gases, and save lives which
wo'oid otherwise be sacrificed.^ Secondly, by means of the instruc-
tion afforded by classes established by the St John Ambulance
Association, miners are learning how best to render firat aid to the
injured before the arrival of a medical man, and there is no doubt
that many valuable lives have been lost in times past for want of
this knowledge. Thirdly, a vast amount of good has been done
by the establishment of Miners' Permanent Relief Societies in
iifferent districts, which afford aid to persons disabled by accidents
and to the dependent relatives of those who have unfortunately
lost their lives by any mining fatalitj-.
16. Useful Minerals produced in Various Parts of the Globe.
Great Britain and Ireland.— The mineral produce of the United
Kingdom for the year 1881 is summed by Mr Robert Hunt* as
follows : —
' From Reports of n.M. Inspectors qf Mines for the year 1882,
p. xxxvi.
' The Rate of Fatal and Non-Fatal Accidents in and about Mines
and on Railmiys, loilh the Cost of Insurance against such Accidents,
by Francis G. P. Nei.ion, London, 1880.
' Reports of H. M. Inspectors of Mines for the year 1881 , Mr
Bell's Report, p. 463.
* Mineral Statistics of the United Kingdom for 1881, p. Ix. ,
Coal.
Zinc ore
Iron pyrites
Gold ore
surer ore
Cobalt and nickel o
Manganese
Wolfram-
Ochre nnd amber...
Arsenic
Fluor spar, Ac
Clays...
Salt..
Bar>-tes
Sundry minerals, including )
coprolltes, gypsmn, calcspar, >
aholes, &c. )
Quantities.
Tons cwts.
154,184,300 0
17,446,065 6
12,898 3
62,556 1
64,703 6
85,627 7
43,616 14
IJ
6 19
63 14
3,884 0
6,166 8
872 14
3,401,421 0
3,398,220 0
65,528,327 10 0
6,201,068 6 6
697,444 5 3
■ 190.057 8 7
6,441 6 0
544 1 B
12,286 7 0
46,070 7 S
2.53 10 0
1,200.210 0 0
1,149.110 0 0
23,894 3 10
349,500 0 0
The totalvalue of minerals produced in 1881 was £76,201,695, Zs.,
exclusive of slate, building-stone, limestone, and other stones worked
by mines and quarries.
The quantity of coal raised in 1882 was 156,499,977 tons.
The metals obtained from the ores produced in the United
Kingdom in 1881 were —
Gold
Sliver, from ore
Sliver, from lead..,,
Pighon
Zinc..'..'.'.'.."'.'.".'.".'.".'.'.'.'.'.'."'..'.'.'
Other metals, estimated...
Total value of metals produced in 1881..
Quantities.
8,875
48,567
14,947
The total value of minerals and metals obtained from the mines
and other mineral workings of the United Kingdom in 1881 was
Minerals, not reduced— salt, days, Ac 2.817,652
£90,860,487
From these tables it is evident that coal and iron are by far the
most important mineral productions of the United Kingdom, as 94
per cent, of the total value is due to these two substances.
France. — The mineral productions of France' for the year 1880 are
set forth in the following table: —
Quantities.
Values.
Mineral fuel
Metric Tons.
19,362.000
248,000
144,000
2,871,000
133,000
63.000
S33.000
367.000)
Francs.
21S.CS7.000
2v-.5.S,0C0
1.023.000
H.9I».000
2.114.000
4.:m.ooo
U.SH.OOO
6,719.000
Bay-salt _
23.514.000
290,711,000
* Statistique de V Industrie Mmirale et d^s Appareils d Vapemr <
Prance et en AlgSrie, Annie 1380, Paris, 1882, p. 45.
468
M 3 N T N G-.
[mineral riioD0CE or
Tho quantities of metal produced in France from native and
ionign ores in 1S80* were —
pffftron^ 1,725,000 metric tons. ' I "NickeL SO metric tons.
Lead. .... 6t500 „ ^ Gold 31 kilogruiumes
Copper.L 3,400 „ „ Silver 40,400 „
jOncL 10,200 „ „ 1 Alumiiiiura 1,150 „
Germany. — The mining industry of the German empire is of
high importance. The output of the mines in 1881 is shown hy
the following table, — taken from the Stat. Jahrb. fur das Deutsche
Reich, Berlin, 1883, p. 27. The proiiuction of common salt,
potassium chloride, and other salts from brine is also considerable.
The total quantity for the German empire in 1881 was 693,000
metric tone, worth 33,507,000 marks, including 113,200 tons of
potassium chloride valued at 14,090,000 marks.
Coal.
Lignite.
Rock-
salt.
Potash
Salts.
Iron Ore.
Zinc
Ore.
I-cad
Ore.
Copper
Ore.
Sil-.-cr
and
Gold
Ore.
Iron PyrilC!
and otli.-i
Vitriol and
Alum Ores.
Otticr
Mining
Products.
Toral Value
ol all the
Mining
Products.
Unit
1000
Sletl-ic
Tons.
Unit
1000
Jletric
Tons.
Unit
1000
lletric
Tons.
Unit
1000
Metric
Tons.
Unit
1000
Metric
Tons.
Unit
1000
Metric
Tuns.
Unit
1000
Metric
Tons.
Unit
1000
Metric
Tons.
Unit
1000
Metric
Unit
1000
Jlclric
Tons.
Unit
1000
Mclric
Tons.
Unit
1000
.Marks.
Prussia'
43760-5
619-8
3707-3
"9-4
■"0-9
108-9
560-9
10412-2
13-1
600-7
'30-7
12-3
735-3
273-7
766-1
"3-2
207-8
0-9
84'2
19-0
645-4
360-5
3906-3
75-6
23-8
193
133-3
28-4
964
32-3
1096-0
669-2
'03
169-7
0-8
1-!
'0-9
1-4
'0-3
623-6
o-o>
01
0-1
26-7
1-12-0
11
0-1
0-1
'04
2-4
33-2
15
12
b'-'o »
0-6
1-4
18-0
2-1
(i'o»
9-7
S2C,42-J
5,124
33,057
752
110
1,115
*S
1,626
1,678
6,344
""5
170
6,690
Bavju-in
Saxonv*
Budcn
Hesse
Tlmriniria
Brunswick
Alaacc-Lorrftinc
48C88-2
12852-3
311-9
905-9
6411-9
2161-9
C59-5
1C4-3
523-7
26-S
146-1 1 67-7
384,000
4,994
Liuemburg -...
Together
48688-2
12862-3
311-9
905-9
7673-8
659-5
104-S
623-7
26-S
HC-1
67-7
5S8,9W
Austria-Hungary. — Among the famous mines of the Austria-
feungarian empire may he mentioned those of Hungary and
Transylvania for gold and silver ; Stj-i-ia produces much of the iron ;
qnicksUver is yielded by the mines of Idria in Carniola, lead and
silver by those of Przibi-am in Bohemia ; salt is obtained in the
Austrian Alps and in Galicia, which also produces petroleum and
ozokerite.
The production of minerals and metals in Austria'' during the
year 1881 was as follows : —
Ooldc
SlWcr ore
Xiuicksilvi
Copper 01
764 metric tons— Metallic gold 18-6 kilogrammes.
2,383 „ „ — „ silver 31,359 „
8,204 „ „ — „ mercui-y„ 398 metric tons.
— „ copper 481 „ „
4,119
618.903
Lead ore 13,542
Zinc ore 27.339
Margancso ore 9.109
Oraphite ia379 „ „
'Petroleum 1,249 „ „
Lignite. 8.961,493 „ „
CoaI_ 6,343,315 „
Exclusive of salt, the value of the produce of the Austi-ian mines
fai 1881 was 44,693,692 florins. The total output of salt in 1881
,was 267,279 metric tons, valued according to tho monopoly prices
at 23,000,493 florins.
Hungary in 1879' produced
Iron 118.321 metric tons.
Coal 674.003 ., „
Lignite... 932.475 „
Iron pyrites 66,292 „
Gold 1.593 kilogr.lr
Silver 1S,C60 „
Copper 1.035 metric tons.
Lead 1,967 „ ,,
Mcrcui-y 22 „ „
TJcJjiiim.— Belgium is rich in coal, the output in 1881 being no
less than 16,873,961 metric tons, valued at 163,704,242 francs.
Though it produces iron ores, it is largely dependent upon other
countries, and especially the grand-duchy of Luxemburg, for supplies
for its blast furnaces. The principal lead mine is that of Bleiberg,
p,ni tho calamine deposits iu the neutral territory of Moresnct have
Jong been worked with success by the celebrated Vieille Montagne
Company, which also ow-ns zinc mines in Belgium, Germany,
Sweden, Sardinia, and Algeria.
Russia. — In a vast empire like Russia it is not surprising that
there should be valuable deposits of a great variety of minerals.
lAinoug tlie most important are the auriferous alluvia of the Ural
inoimUins aud Siberia, which in 1880 yielded 115,940 troy lb of
gold, worth more than 5 millions sterling. Platinum is found associ-
ated with the gold-bearing sands of the Urals ; the outiiut in 18S0
»vas 7895 troy lb. Zinc ore is largely worked in Poland. Iniport-
n France et en
'"bcUUcd'statlstlcs concerning' tlie mineral priidncc of Prussia ape given ever>-
.ycnr In the Zetlscltri/I /Hr ial Bern-, Uutten-. unit Salinm- IITioi im J'rauiia.lieil
Staalc (Devlin).
a Quantity less than 60 tons.
* Detailed Btittlslics of tho mineral produce of Saxony are given ycanv In the
Uoftrft/if/i fiir dtit Berg- und tliiltenveun^im RUttlireiehc 5rtf/r*(-M(Frclbcrg).
6 SMI. .lahrb. da t. i. Aderbau- JtiniiUrlumi /ur 1681, licit 111., Lle(. 1,
'Vienna. 1RS2.
8 " Dcr Bergwcrksbctrieb Ungams Im Jahrc 1879," Oesterreiehitetie ZcitKhri/t
JUr Bern- und Uiidemiam, 1881, p. J71.
ant su]tplies of chi-omic ij-on ore are derived from the Urals, amount-
ing iu 1880 to more than 8000 tons. The metallic copper produced
in 1880 was .about 3100 tons, and the oil wells of Baku yielded iu
that year 346,000 tons of petroleum. Kussia also possesses mines
of ii'on ore, mariganese, lead, silver, coal, and lignite. A little tin
ore is furnished by Finland. ;
Italy. — The most important mineral iu Italy^ is sulphur, 359,540
tons (metric), worth 36,448,453 lu-e, having been obtained in 1880,
and mainly from seams containing the native element in the
Miocene rocks of Sicily and Romagiia. ^
The celebrated iron mines of the island of Elba have been worked
from very early times, and furnish a valuable ore ; and the deposits
of calamine, lead ore, and silver ore in Sardinia form no small pro-
portion of the mineral wealth of the Italian kingdom. The g.i' J
mines in and near the Val An7asca (Piedmout) aie producing nioiij
than 7000 ounces of metal yearly. - '
Spain.— S^MU is justly celebrated for its miner,il wealth. It-
produces more cupieous pyrites than any other country in the world,
and very large amounts of lead ore and quicksilver; and its iron ores'
are abundant and of excellent quality. The principal lead mines
are in the provinces of Jaen (Andalusia) and Slurcia, and tho total!
amount of metallic lead produced in Spain or from Spanish ores i»
estimated to be 120,000 tons yearly.
Cinnabar, the heavy red ore of mercury, naturally attracted atten-
tion at a very early date, and the w-orld-renow-ned Almaden mine
has been w-orked from time immemorial. The output in 1880 w,as.
13S7i tons (metric) of quicksilver.'
Tlie cupreous pyrites, often known as sulphur ore, is obtained
from the province of Huelva, where vast deposits occur over a belt of
country nearly 100 miles long by 20 miles wide. The Rio Tinto
mines are the largest in the district, and are worked on a gigantic
scale. Tho company employs upwards of 10,000 hands, or raoix-
persons than are engaged in oil the Cleveland iron mines, and the
output is upwards of a million tons per annum. About one-quarter
of this, containing 3} per cent, of copper, is exported, mainly for the
manufacture of sulphuric acid and subsequent treatment for copper
aud silver, whilst the remaining thi-cc-quartei^,w-ith 2 J to 2i per cent,
of copper, are treated on the spot. The oiv contains i-athcr less than
1 oz. of silver to the ton, aud a few- gi-.-iins of gold. These arc profitably
cxti-nctcd from the bunit 01-c by Claiulet's process, and some idea of
tlie iinpoi-tance of the copper and silver will be pained by reference
to the following figures." During the year IS.Sl tlicre were obtained
from cupreous pjTitcs imported into the United Kingdom in 1681,
mainly from Spain and Portugal, 14,000 tons of copper, 258,463 oz.
of silver, and 1490 02. of gohl. The total value of tho silver and
gold was £64,195. • . - --•
The total outputof iron ore in 1880 was 3, .565,338 metric tons,"
more than two-thirds, viz.. 2.683,027 tons, being obtained fi-om the
celebrated mines near Bilbao in the province of Biscay. Enghm Ij
France, Belgium, aud Germany are all glad to draw supplies of
7 Koliilr ilalltllelie inlla rnduilrta Jtinernria in Jlalia dot ISOO 0/ ISSO. I:oni».
19S;, p. 400.
s Ettadiiltea ilinera d* Etpa^a, corrtspondtaitt at ana dt 1860, iTatlrid, li9X
p. 37.
» Hnnt. Ulnernl Slalllltei, Ac, p. 15.
1' Sttadiitica i/fncra, &c., til itipra, p. 15.
HVyKnEST COUNTniES.j
excellent red and brown hematite from the Bilbao mines. JIurcia
com<;s next in importance to Biscay, vith a production of 539, 32S
tons,
Portugal. — The great mineral belt of Huelva extends into Portngal,
and deposits of cupreous pyrites almost identical witli that of
Fio Tinto have been wrought from very early ages. The principal
mine, Sau Domingos, is close to the Spanish frontier. It is estimated
Chat the worldngs liad yielded up to the year 1877 no less than
3,678,7'i5 English tons of cupreous pyrites, by far the greater part
of this bavin*; been extracted in recent times. The quantity of ore
raised from tnc mine in 1882 was 405,029 tons.
Portugal possesses notable mar.ganese mines, but produces com-
paratively su;all quantities of iron, lead, and copper.
Koricay. — The mines at Kongsberg are famous for the large
quantities of native silver they produce, and enormous masses are
Bometimes mot with. The annual output is from 10,000 to 12,000
troy ounces. Copper ore and cupreous pyrites are also mined in
Norway, and there are important workings for nickel and cobalt
md for apatite. Alluvial graveb have been washed for gold in
Norwegian Finland.
Sweden. — The most important mineral obtained in Sweden is
iron ore, much being in the form of magnetite ; red hffimatite also
is mined, and brown haematite is dredged up from some of the lakes.
The principal iron-producing districts are those of Norberg, Danne-
mora, Nora, and Ferseberg. The output of the Swedish mines in
1880 was— i"
Iron ore 775,50.5 tons. I Zinc ore 43,452 tons.
Lead ore 12,988 ., I Copper ore 29,380 „
Grecee. — One of the most interesting undertakings of modem
times has been the re-working of the Laurium mines, which are
situated in the southern extremity of Attica ; and an account of them
written by Cordelia furnishes many curious details concerning the
metbodsof mining, washing, and smelting employed by the ancients.
The workings for lead and silver appear to have been carried on
with the greatest vigour between 600 B.C. and the Pcloponnesian
War, and were finally abandoned in the 1st century of fhe Christian
era. Huge piles of slag which had accumulated from the old
smeltiag works were found to be well worth b''ng re-worked for
silver and lead, and operations were commenced in 1864. Five
yeare later the old heaps of mine refuse began to be treated, and at
last in 1375 a French company resumed working the mine. A
Greek company employing some 3000 persons is now producing
annually from the old mine heaps no less than 8000 to 9000 tons
of pig lead, yielding 45 oz. of silver to the ton, whilst the mines of
the Cvimpagixic fra-iuiaise des imnts du Laitrinm made an output in
1881 of ?C,664 tons (metric) of roasted calamine, with 40 to 60 per
cent, of zinc, in addition to lead ore and mixed ores. Cordelia cal-
culates that during the three hundred years the Laurium mines were
worked by the ancients the total amount of lead produced was
2,100,000 tons, with 22i million troy lb of silver. Besides this the
ancients left behind two million tons of lead slags containing on an
average 1067 per cent, of lead, 109 million tons of mine refuse
mth 1 J to 18 per cent, of lead, and excavations to the extent of 51
million cubic yards with lead ore still in sight They did not
touch the calamine deposits.* Next in importance to lead, silver,
and zinc conies bay-^lt, and after that emery. The island of
Naxos furnished 3300 metric tons of emery in 1877, valued at
f28,000.
i Africa, — Algeria is rich in Iron, and three-fourths of the value
of its total mineral output are due to ores of this metal. In
1880 the iron mines produced 614,000 metric tons of ore, Mokta-
el-badid mine, near Bona, alone yielding about 300,000 tons.
Algeria also possesses mines of copper, lead, zinc, and antimony.
The name " Gold Coast " applied to part of the shores of Africa,
denotes its productiveness of the precious metal, and it is prohnble
that very important supplies of gold will one day be derived from
various districts of the Dark Continent.
Cape Colony possesses rich copper mines in the Naraaqualand
division, which in 1882 produced ore and metal worth £331,546;
however, the most valuable and remarkable mineral deposits of
Africa at the present time are the diamond mines. The first
diamonds were obt.incd from recent gravel in the bed of the Vaal
river, and it was afterwards discovered that the precious stones
could be obtained from the so-called dry diggings. The most im-
portant of these, the Colesberg Kopje, now known as the Kimberley
mine, prod-iced in 1881 diamonds weighing 900,000 carats, worth
£1,575,000. Three other neighbouring mines are Old De Beer's,
which yielded 300,000 carats in 1881, worth £600,000, Du Toit's
Pan, and Bulfontein. The value of the diamonds raised in South
Africa since 1870 amounts to forty millions sterling ;- indeed the
Kimberley mine alone was estimated in 1877 to have already pro-
duced ten million pounds worth of diamonds, extracted from 4
million tons of diamantiferous rock.
MINING
4e£i
1 A, Cordelia. " MincraloEisch-eaolociBChe Reiscskizzeo aus Griechcnland,"
htrg- und hOltenma'tiii'f^e Ztttung, vol. xli!., 1883, p. 21.
' A. J. Mac'laiial'l. "The Value of the Cape as a Dependency of Great Britain."
.<4^.— For many centuries India was regarded aa poflsesaiog
fabulous mineral wealth, and a strong basis for this idea may be
found in the existence of traces of mining on a very extensive scal^
No doubt in early days India did supply what then appeared to b*
very large quantities of metals, and a country that produces gold
and precious stones is apt to be endowed by the popular mind with
boundless riches. The actual amounts of mineral raised in India
at the present day are comparatively small. Cold exists over con-
siderable areas, but it remains to be proved that the gold minee of
the Wynaad and Mysore can be proijtably worked by British com-
panies. Diamonds occur and are worked in alluvial diggings
and in a conglomerate belonging to the Vindhyan formation.
Sapphires and rubies are obtained from Upper Burmah. Ceylon*
produced in 18S0 no less than 10,286 tons of graphite or plumbago,
valued at £192,879. Petroleum is abundant in Upper Burmah, and
oil from wells has been utilized for upwards of twenty centuries.
The total output in 1873 was estimated to be about 10,000 tons
yearly. Tin ore occurs and is worked in Tenasserira. Passing into
Siam and the Malay Peninsula we find deposits of alluvial tin ore,
producing what is known in commeree as Straits tin. A littla to
the east are the islands of Banca and Billitou, which for many years
have been a source of wealth to the Dutch Government. The sales
of Banca tin in 1881 amounted to 4339 tons, and those of Billiton tin
to 4735 tons, whilst 11,475 tons of Straits tin were exported from
Penang and Singapore.^ Stanniferous alluvia are also worked iu
Karimon, Singkep, and Sumatra, whilst the latter island possesses
also valuable seams of coal.
Borneo furnishes coal, antimony ore, and soma cinnabar; aai
river-graveb are washed for diamonds, gold, and platinum.
There is no doubt that the mineral wealth of China is enormoua.
In addition to important coal-fields it possesses numerous metallio
mines. The province of Yunnan in the south of the empire seems
to be specially favoured with regard to metalliferous wealth, f«
mines of gold, silver, copper, lead, tin, and iron are worked there,
whilst jade and precious stones are found in the beds of rivers.
Japan produces more than 3000 tons of copper yearly, or about aa
much as the British Isles. The output of lead and tin is insignifi-
cant, but the quantity of silver, exceeding 300,000 oz. yearly, is
worthy of notice. Gold, iron, and petroleum are other products of
Japan. >y'
The gold of Siberia has been mentioned in speaking of Russia. *
Canada. — The Dominion of Canada is rich in minerals. Gold-
bearing quartz veins are worked in Nova Scotia, whilst in British
Columbia alluvial deposits are the main source of the supply.
Silver occurs on Lake Superior, the most important mine being that
of Silver Islet, which from 1869 to the spring of 1877 yielded 2i
million ounces of silver, and gave a profit of £200,000.
Rocks resembling the copper-bearing strata of the United States
territory are mined in Slichipoten island in Lake Superior. Iron
ores, in the form of magnetite, red hematite, limouite, and ilmeaite,
arc worked in various parts of Canada.
Petroleum is derived from oil wells iu Western Ontario, and th#
quantity refined in 1875 was about 210,000 bairels, each of 40
gallons. It is in Ontario also that the veins of apatite exist from
which a large amount of that useful mineral has been raised.
UniUd Stales.— The mineral wealth of the United States is
admirably summed up by Mr Kichan' P. Rothwell in his addres*
to the Americau Institute of Mining Engineers.'
"Production of Coal, Metal, and Petroleum in 1881.*
Anthmcite 30.261,940 tons (of 2240 ll>).
Bituminous coal 42.417,764 „ (of 2000 lb).
Pig iron 4,144.000 „ (of 2240 a,).
Lead 105,000 „
Copper 1 81.000 .. „
Quicksilver 59,000 flasks (of 761 !!>■ a^o^
Gold 831.870.000 (=I,541,7'I oi.).
Silver. 845.078.000 (=34.865.900 oz.).
Petroleum 27,204.000 barrels (of 42 gullonfi).
" Tlie statistics of other nsefnl minerals and mclals show an equally marTeJteas
advance during the past thirty years. The production of pic iron, which in ISSt
was 541,000 net tons, in 1361 was 653,000 tons, and In 1S71 was 1,70S.OOO tcjis.
Ten years later, in 1881, we produced no less than 4,141.000 tons, on increajo la
thirty yeara of nearly 800 per cent.
" Lead, which appears at 14.400 tons in 1852, varied but little from that fignpe
until the construction of railroads into the arcentifcrous lead-mining districts of
the west about 1870. Eurel<a, Nevada, Utah, and moi-c recently Colorado, witjl
its Leadvillo bonanzas, rapidly raised the production from 18,000 tons in 1871 1*
47,000 tons inl8;3, 75,000 tons in 1877, and los.ooe tons In 1881.
••Our production of copper steadily increased rom 1000 'ons in 1852 to 31,000
tons in 1881,— the enormous output of that unr .-ailed mine Calumet and HecU
steadying the production and neutralizing the 6: tu.-itions of the lesser mines.
" Quicksilver has shown wide fluctuations, du -
to the condition of the i
3 Slalisllcal AbUracl/or Ihe Several Colmia! and other Poueitiim of lie UnlUd
Kingdom in each pear from 1860 to 18S0, London, 1SS2, p. 59.
* Hunt. Uirt. Slat, for 1881. p. 9.
5 Engineering and Mininy journal, vol. xxxlv. p. 174.
6 The total produrtioa of coal in tiie United Slates in 1SS2 araovmed M
86,562.614 tons of 2240 lb iCoUiery Guardian for 16S3. p. 7S1). The ijuantiUea of
metals produced in 1882 are estimated to be— pig iron 4,623,323 crost Uv*^
2240 tb each, lead 123,000 gross tons, copper 40.000 gross tons (r/« /ran, JM«,«»*
Alhti Trada in 1882, p. IS3 ; £«■}. and Mm. Jour., vol. xsxv. p. HX
470
MINING
[3XINBKAL PBODUCB Gl
|»Ute IV.
bnt it went C9 low ar 10.000 flaplcft In IPSO, and roso to 6S.0W flfwks five ycaro
Iftter; from tlili It decUned to 16,000 fiutu 1q 187A. thoQgh in the foUo^^log >ciir
U grew to 76.000 flaaks. Last year we produced 69,000 flasks.
•' Gold l3 the only metal tn which cor production Ijas been dccllninR. In 1S52
It amounted la gtiO.OOO.OOO ; bat, vrltli some flactuatloas, it liaa now declined to
leas than 532.000,000 unnually.
*'Tho production oi silver, on tbe contrary, liua lorccly incrwwed. Commenc-
ing in 1859 with 8100.000, it ha3 now attained S-15,000,000. In 1S77 only were
these flgiires esceeded, and then only by about $1,000,000.
"Tho production of petroleumf that creat American Industry, has grown wKb
wonderful rapidity. In 1859 it commenced with only 3U00 bairels, and, a/ter an
almost uniform Increase, it attained last year the cnonnous figures of '27,000,000
exhaustion."
Some valuable statistics concerning the production of tbe pi
metals in the United States are contained in a report issued by the
Census Bureau.* The output for the year ended 31st May 1880 is
£ummed np qs follows :-
Gold.
SUvcr.
Total.
Oance8.
Value.
Ounces.
Value.
Value.
Deep mines....
1,033.974
580,767
$21,374,152
12,005,511
31,717,297
80,177
841,007,296
103,661
£62.331,446
12,109,172
AH mlDC&
1.614,7-11
33.379,663
31,797,4W
41.110,957
74,490,620
The State producing the gi-eatest value is Colorado, viz.,
$19,249,172, or gold 130,607 02. and silver 12,800,119 oz. ; Cali-
fornia comes next, having produced $18,301,828 of bullion, and then
Nevada, with $17,318,909 of bullion.
The greatest gold jiroducer among the States and Territories is
California, with 829,676 oz. of gold, half from deep mines and half
from placers. Next follows Nevada, with 236,468 oz. of gold, of
iWliich only about 1 per cent, came from placer mines ; then Dakota,
159,920 oz. of gold, nearly entirely produced by deep mines ; and in
the fourth rank Colorado, 130,607 oz., with a olacer production of
Jess than 5000 oz.
The greatest silver producer is Colorado, with 12,800,119 oz. ;
*hen Nevada, 9,614,561 oz.; then Utah, 3,668,365 oz.; Montana,
2,246,933 oz. ; and fifthly Arizona, 1,798,920 oz.
It is useless within the limits of this article to attempt to convey
an adequate idea of the enormous mineral resources of the United
States. We can merely very briefly allud-o to some of the principal
deposits, which are of coniniercial value on account of their magni-
tude, of scientific interest owing to their mode of occurrence, and of
itechnical importance as having led to the introduction of consider-
able improvements in the arts of mining, milling, and dressing.
Among these may be mentioned the coal and anthracite mines
and oil wells of Pennsylvania, the gold and quicksilver mines of
California, the silver mines of Nevada, the lead and silver mines
of Colorado, and the copper mines of Lake Superior. The articles
Coal (vol. vi. p. 60) and Gold (v.ol. x. p. 743) may be referred to
for information concerning the occurrence of these minerals and
the method of extracting gold by hydraulic mining and improved
stamping machinery.
Quicksilver in the form of native mercury and cinnabar occurs in
considerable abundance in CaliEomia, and much of it is found in
coniexion with serpentine, either in the serpentine itself or in sand-
stone near its junction with serpentine. The most important mines
ere those of New Almaden in the southern part of the State near
San Jose. The deposit at Sulphur Bank in Lake County is of much
geological interest. It consists of native sulphur, gypsimi, and
cinnabar In a decomposed andesitic lava close to an extinct geyser
from which boiling water still issues. Tlie top of the bank was
worked open-cast for sulphur, and" then for sulphur and cinnabar,
and now underground mining is carried on in stratified sandstone
and shale impregnated with cinnabar and underlying the lava.
Some of the most marvellous silver mines in the world are those
upon the Comstock lode in Nevada. A horizontal section of pai-t
of this great vein is shown on Plate IV., copied from the excellent
and wetl-known report of Jlr J. D. Hague,* The strike is nearly
north and south, and the dip about 43° to the east. "The vein
matter of the Conisto-ik consists of cmshed and decomposed
country rock, clay, and quartz." "Up to January 1, 1880, the
Comstock had yielded in twenty years about §325,000,000 worth
of bullion. The total length of shafts and galleries is about
250 miles. The number of men employed in the mines in January
!l880 was 2800, earning average wages of $4 a day. At the .same
Idate 340 men were at work in the amalgamating mills." ^ The
'heat of the Comstock lode is remarkable. On the 2700 feet level
of the Yellow Jacket mine Mr Becker found the temperature of the
iwater to be 153", that of the air 126" ; whilst the water in the Yellow
Jacket shaft at adi-pth of 3065 feet has a temperature of 170" Fahr.*
' aarcnco King, Bpecial agent of the Ccnfius, Slatisties 0/ the Production 0/ the
JYecious Mctalt in the Vnittd Slatei, WaslilnRton. 18S1, p. 69.
, « United States Geological Exploration 0/ the Fortieth ParalM, vol. UL, Mining
Induatiy, Atlns. plate 11.
8 Clarenco King, Firit Annual Report ofth* U.S. Qceicgiial Survty, v. 3J.
^(^CU^ pp. 44, 45.
During the last few years the Comstock lode ha? been falling off
in productivencES. Ln 1876 tlie total yield of the Comstock lode
was §38,572,984 (gold, $18,002,906; silver, 520,570,076). During
the census year ending May 31, 1380, the product of the whole
Comstock district, including outlying veins, was $6,922,330 (gold,
§3,109,156; silver, $3,813,174), showing a decline of $31,650,654,
or 82-06 per cent., since 1876.^
Though the extraction of silver from its ores may bo regarded
as Iho business of the metallurgist rather than of the miner, we
must not forget to mention that it is to the necessities of the treat-
ment of the Nevada ores that we owe the system of pan amalgama-
tion first developed in that State and practised since in Colorado.
Another district in Nevada which cannot be passed over in
silence is that which contains the Eureka and Richmond mines, which
are celebrated, not only for the silver they have produced, but also
for the important trial in which the issue hinged upon the defini-
tion of the term vein or lode (p. 441). The bullion produced in the
Eureka district from ore raised and treated during the census year
ended May 31, 1880, was— gold, 62,893 oz.; and silver, 2,037.666
oz. ; worth altogether $3,934,621.^
The history of Leadville in Colorado seems like a romance when
we read of the rapid development of the mines, the creation of a
large and important town, the erection of smelting works and the
building of railways, under very adverse conditions, in the heart of
the Rocky Mountains, all within the space of four or five years. It
affords additional proof that the miner is the true pioneer ol
civilization. The main facts concerning the Leadville deposits ai-o
admirably summed up by Mr S. F. Emmons, from whose report"
we borrow, not only the following facts, but also the geological
section across the district (Plate IV.).
The principal deposits of the region are found at or near the
junction of the porphyry with the Blue limestone, which is the
lowest member of the Carboniferous fonnation. This bed is about
150 or 200 feet thick, and consists of dark blue dolomitic limestone.
At the top there are concretions of black chert. The porphyry
occurs in mtrusive sheets which generally follow the bedding, and
almost invariably a white porphyry is found overlying the Blue
limestone. This porphyry is of Secondary age ; it is a white homo-
geneous-looking rock, composed of quarlz and felspar of even
granular texture, in which the porphyritic ingredients, which are
accidental rather than essential, are small rectangular crystals of
white felspar, occasional double pyramids of quartz, and fresh hexa-
gonal plates of biotite or black mica. Along the plane of contnct
with the porphyry the limestone has been transformed, by a process
of gradual replacement, into a vein consisting of argentiferous
galena, cerussite, and cerargyrite mixed with the hydrons oxides of
iron and manganese, chert, granular cavernous quartz, clay, heavy
spar, and "Chinese talc," a silicate and sulphate of alumina. Tbe
vein seems to have been formed by aqueous solutions, which took
up their contents from the neighbouring eruptive rocks and brought
about tlie alteration of the limestone as they percolated downwards
through it. In Carbonate Hill, a gradual passage may be observed
from dolomite into earthy oxides of iron and manganese. The inasscs
of workable ore are extremely iiTegular in shape, size, and distribu-
tion. They are often 30 to 40 feet thick vertically, and occ^isionally
80 feet, but only over a small area. The ricli ore bodies are common-
est in the upper part of the ore-bearin» stratum. At Fryer Hill
the Blue limestone is almost entirely replaced by vein material.
In the census year ended May 31, 1880, Lake County, Colorado,
which includes the Leadville district, produced 28,226 gross tons of
lead, with 3830 oz. of gold and 8,853,946 oz, of silver, of a total
value of $13,032,464.8
The most important copper mines of the United States are those
on Lake Superior, where the native metal occurs "in veins, in large
masses, or scattered more or less uniformly in certain beds which
are either amygdaloid or conglomerates."" The principal copper-
producing districts are in Michigan, where the Portage Lake dis-
trict, in Houghton county, contams the famous Calumet and Hecla
mine, whicli alone protluced 15,837 tons of copper in 1880, or about
Italf the entire output of the United States. The deposit from
whence this vast amount of copper was obtained is a bed of con-
glomerate, generally called a vein, dipping about 38*^ north-west
It has been worked for a depth of 2250 fe*t on the incline. lu
]S75 the stuff stamped yielded 4^ i>er cent, nf copper.
In conclusion, we will point out that the value of the mining
inlustry in the United States exceeds that of any other country in
the world, Mr Porter estimating it for 1879-1880 at 360 million
dollars, and that of Great Britain at 325 millions.'** Germany holds
» Clarence Kinr, Statistics of the Produttion of the Precious Melali in tht
United States, Washington, 18S1, p. 19.
» Ahifraet of a Report vpon the OeoJcgy and Mining Indvttry 0/ Liadttil},
Colorado, Washlncton. 18S2.
8 Clorcnco King, op. eit.. p. 47. -
9 Charles E. Wilght, commissioner, Annual Report Of the. Commissioner ^
if tnerat Stalisties forihe State of Michigan for \SSO, Lenslng. Michlgau, I8»l,
" Robcit V. Porter, The Wat from the Census of 1880. Chicago and Loodoo,
1882, p. 19.
©ITFEEENT COCmTRlES.] M i ^ i JN AT
tho third rank, followed by France and RnssiaT Tffc United States
iiroduce 33 iier cent.' of the gold yield of the whole world, 60 per
cent, of tho silver, 22 per cent, of the pig iron,' 29 per cent, of the
s*ccl, ar.d about 25 per cent, of the leaxL
Afarico has been renowned for its gold and silver mines ever since
iha Spaniards first took possession cf it, and its production is still
very consi derable. Indeed, after tho United States, it still produces
far more silver than any other country in the world. The average
annual output of silver daring the twenty-five years 1851 to 18/5
is estimated by Dr Adolf Soetbeer at 601,520 kilogrammes, or
16 124 235 oz. ;' whilst tho average annual output of gold during
the same period was 1785 kilogrammes, or 57,389 oz. Tm ore
occurs in considerable quantities in Mexico, and is Ukely to be
worked on a large scale as soon as the tin district is opened up by
a r.iihvay. .
Central Ama-ica possesses numerous gold mines.
South /tmerwa.— Venezuela produces gold, copper, and a little
lead The copper is found at Aroa near the north coast, and the
cold in the province of Guiana, which is now producing upwards of
100 000 oz. annually. It is highly probable that the existence of
this gold was known to the Indians, who reported it to Sir Walter
Ralefoh, and so led him to undertake his unfortunate c^qDedition in
search of *' El Dorado. " French Guiana contains workable deposits
of Kol<l, and yielded 72,168 oz. in 1880.
The chain of the .iVndEs forms a long belt of mineral-producing
country. Beginning with the United States of Colombia we have
a country rich in gold,— the State of Antiquoia being especially
favoured in this resnect. The annual yield of all the states is about
205,000 oz. Colom'hia has mines of rock salt, yielding 19,000 tons
a year, and tho emerald mine at iluzo has long been famous. Peru
is renowned for its silver mines ; tho br>st-known are those of Cerro
,ie Pa2C0, situated at an elevation of 14,000 feet above the sea-level.
Passing into Bolivia, we must notice the silver mines of Potosi,
the wcilth of which is proverbial. Chili is best known as tho
principal copper-producing country of South America ; but its silver
mines are not unimportant, and beds of nitrate of soda are largely
wrought
The most remarkable gold mines of Brazil lie in the province r i
Minas Geraes, whilst diamonds aro obtained in that of Matt
Grbsso. In the Argentine Kepubiic gold, silver, and copper miiici
are worked, especially in tlie provinces on tie eastern Hanks of the
Andes. , . „
i The total annual output of the precious metal in South America
is estimated to be upwards of 300,000 oz. of gold, and 2,000,000 oz.
of silver. In 1877 Chili exported 35,128 metric tons of metallic
copper, in addition to ore ana regulus.
A uMralia. — Australia is remarkably rich in minerals, especially
gold (see Gold, vol. x. p. 744), tin, and copper, and its coal deposits
are likely to be largely utilized in the future.
Queensland, though a young colony, has already made itself
famous for gold and tin, and it also possesses vast resources of coal
and copper, in addition to the ores of other metals. The quantity
of gold sent by escort from the difTerent gold fields was 204,388 oz.
in 1880, in addition to what was carried by private hands. Tin ore
was first vforked in 1872 near the border of tho colony with New
Couth Wales, and large quantities of stream tin have been obtained
from very shallow alluvial diggings near Stanthorpe. Like gold,
47J
the tin ore is not confined to one district ; it occurs and ia worked
at the North Talmer diggings; a little to the south ia Great
Western, rich in tin ora, and so is Herberton to the north-cast on
the other side of the Dividing range.
In 1831 New South Wales* proujced minrttds and metals worth
£2,373,191, viz., 149,627 oz. of gold, 1,775,224 tons of coal, 8200
tons of tin, 5493 tons of copper, 6560 tons of iron, besides silver,
oil-shale, and antimony. In addition to the facts concerning the
occurrence of gold already mentioned (loc, eit.), it is interesting to
note that auriferous conglomerates containing the precious metal in
payable quantities have been discovered and worked in this colony
in rocks of the age of the Coal Measures.' The most importanttin
district is that of Vegetable Creek in New England, which from
1872 tp 1880 produced 20,988 tons of tin ore. The accompanying
map (fig. 105*) shows the recent alluvium which has hitherto been
Fio 105. -Sketch Map of Part of Vegetable Creek, New South Wales,
show-ing recent and ancient tin deposits. The stippled part re-
presenU tin-bearing alluvium. The shaded part AB denotes
basalt which has covered the lower portions of the i^ient tin-
bearing alluvia (deep leads), ss explained in fig. 106. The rest is
granite,
the main source of the supply, and the deep leads which, as far as
xplored at present, promise still greater riches. The section (hg.
06 «) shows that these deep leads, Uke those of the gold fields
106 «)
Deep Lead,
ftbout 1^0 ft. Oeep,
Fio. lOS.— l^arged Section (on AB of fig. 105) across Deep Leads in Vegetable Creek, New South Wales.
(QOU), T6L x.p. 743), are old alluvia preserved under a capping of I mines now at work are on Yorke's Peninsula. In 1881' South
basaltic lava. There are also numerous tin lodes which are begin- Australia produced 3S24 tons of copper, worth £263,370, and 21,638
nii:g to be worked. ! tons of copper ore, worth £154,926.
Victoria heads tho list of gold-producing British colonies, having I In 1881 Western Australia exported 1400 tons of lead ore, valued
viplded in 13S2'' as much as 864,610 oz., of which 352,078 oz. were I at £11,204.
derived from Ulavial deposits, and 512,532 oz. from quartz mines. I Tasmania, like some parts of Australia, is rich in tin ore, which
1077 tons of tin ore were raised and 375 tons of antimony ore. I is now obtained principally from an alluvial deposit at Mount
. South Ansti-alia is the great copper-producing province, though j BischofL The ore is now^almost entirely smelted ^°_^*f ^f'^°J°°y;^^J
the yield is not so great as it was ten years ago. Tho principal ' '' ' ""'"' ^ c — -*- »« /,«o/i ^rp wn
' Clarence King, op. cit., p. 93.
> James M. Swank, Siaiuucs ff tht Inn caul Sltd Pradnctimi <iftht Vnttcd
StaUi, Washini^on, 18S1, p. 179.
• Dr AdoU Soeibeer, BJilmtlaU-Pniuttioit, Ootlia, 1879, p. SO.
« Artntutl Rtport of the Department ttf Mine*, Neie South Walet.for the year
1881. Melboume, 1882, p. 6.
» Annual Report of the Department ofjfines, 2few South Wetter for the tear
]S;6, Syilney, 1877, p. i;3.
• Furnished by Mr W. H- Wesley.
7 Hiner'- StatUtiei of Tleloriafoi- the ieor ISSt, MellKranie, 1883, p. 7.
in 1880 the exports were 3951 tons of metal and 3 tons of ore, worth
altogether £341,736.
tleta .^coZaiui furnishes a considerable amount of gold from quartz
reefs and alluvial diggings. The annual exports during the ten
years 1862 to 1872 were often 600,000 and even 700,000 oz. Of late
years the yield has gradually diminished, and in 1880 only 303,215
oz. , valued at £1,220,263, were exported. Silver is exported to the
' acXUticaX BrgUter of the Protirue of South Australia for the tear 188J,
Adelaide, 1882.
472
M I N — M I N
extent of 20,000 to 30,000 oz. aunually ; it is mainly derived from
the gold obtuincd iu the Thames district, which contains about 80
per cent, of the less valuable metal. Coal is worked in several
places, but the total output is at present comparatively small.
New Caledonia. — The discovery of nickel ore in this island by
M. Gamier in 1867 was one of great mineralogical interest, and it
has since borne fruits of considerable commercial importance. The
New Caledonia ores are hydrous silicates of nickel and magnesium,
which occur iu veins in serpentine, and contain from 7 to 18 per
cent, of metal. The mineral is found on the Mont d'Or not far
from Noumea. Most of the ore is sent to France to be treated.
To the list of worfcs on tnlaloi: meotloned in tho article Coal (rol. vt p. 80'
the following may bo added :— Cullon, Court ctriploilalion del ilina, furiv
1874, and English translation by C. Le Neve foster and W. Galloway; Serl*.
Leil/ttden zur Berglatikmitt, BCTJIn. 1876; Zoppcltl, Arlt mincraria, Milan,
18S2 ; A. von Groddecl(, Die Lehre von den Lagentdtten der Erze, Lelpaic, 1879 ;
P. von Kittinger, Lehi-tmch der Aufbertitungsktinde, Berlin, 1867 ; Jahrimch fOr
das Berg- und Hiiltenwesen im Kiinigrtiche Saehsen, Freiberg, annually; AnnucU
Reports of JIM. Jmpectora of Mines; PreJiminary Report of Her Afniesly't
Commissiomrs Appointed to Inquire into Aeeidents in Mines, London, 1861;
Annates des Mines, Paris, 6 parts published yearly ; The Engineerin.j and Mining
Journal, New York, pablished weeitly ; Trattsaetions of Ifie Ameriean Institute of
Mining Engineers, Philadelphia ; IHe berg- und huttenntdnnische Zeitung, Leipslc,
weelily; Oeslerrcielii;ehe Zcitsehiifl fUr Berg- und Uiittenwesm, Vienna,
weekly. (C. L. N. F.) .
, MEKISTEY. Ever since the introduction of monarchical
institutions into England the sovereign has always been
surrounded by a select body of confidential advisers to
assist the crown in the government of the country. At
no period could a king of England act, according to law,
without advice in the public concerns of the kingdom ;
tho institution of the crown of England and the insti-
tution of the privy council are coeval. At the era of
the Norman Conquest the king's council, ot as it is now
called the privy council, was composed of certain select
members of the aristocracy and great officers of state,
specially summoned by the crown, with whom the sove-
reign usually advised in matters of state and government.
In the earlier stages of English constitutional history
the king's councillors, as confidential servants of the
monarch, were present at every meeting of parUament in
order to advise upon matters judicial in the House of
Lords; but in the reign of Richard II. the privy coun-
cil dissolved its judicial connexion with the peers and
assumed an independent jurisdiction of its own. It was
in the reign of Henry VI. that the king's council first
a.ssumed the name of privy council, and it was also during
the minority of this sovereign that a select council was
gradually emerging from out of the larger body of the
privy council, which ultimately resulted in the institution
of the modern cabinet. Since the Revolution of 168S, and
the development of the system of parliamentary govern-
ment, the privy council has dwindled into comparative
insignificance when contrasted with its original authorita-
tive position. The power once swayed by the privj' council
is now exercised by that unrecognized select committee of
tho council which we call the cabinet. The practice of
consulting a few confidential advisers instead of the whole
privy council had been resorted to by English monarchs
from a very early period ; but the first mention of the term
cabinet council iu contradistinction to privy council occurs
in the reign of Charles I., when the burden of state affairs
iwas intrusted to the committee of state which Clarendon
pays .was en^-iously called the " cabinet council." At first
government by cabinet was as unpopular as it was irregular.
Until the formation of the first parliamentary ministry by
William III. the ministers of the king occupied no
recognized position in the House of Commons; it was
indeed a moot point whether they were entitled to sit at
all in the lower chamber, and they were seldom of one
mind in tho administration of matters of importance.
Before the Revolution of 16S8 there were ministers, but
no ministry in the modem sense of the Word ; colleagne
Bchemed against colleague in the council chamber, and it
w'as no uncommon thing to see ministers opposing one
another in parliament upon measures that ought to have
Ibecn supported by a united cabinet. As the exchange
from government by prerogative to government by parlia-
ment, consequent upon the Revolution of 1688, developed,
and the Hou.se of Commons became more and more the
-.'entre and force of the state, the advantage of having
ministers in the legislature to explain and defend the
measures and policy of the executive Government becMin
gradually to be appreciated/ The public authonty of thei
crown being only cxercLsed in acts of administration, or, in
other words, through the medium of ministers, it became
absolutely necessary that the advisers of the sovereign,
who were responsible for every public act of the crown as
well as for the general policy they had been caUed upon to
administer, should have seats in both Houses of Parliament.
The presence of ministers in the legislature was the natural
consequence of the substitution of government by parli#
ment for the order of things that had existed before 1688.'
StiU nearly a century had to elapse before political
unanimity in the cabinet was recognized as a pohtical
maxim. From the first parliamentary ministry of WiUiam
III. imtU the rise of the second Pitt divisions in the cabinet
were constantly occurring, and a prime minister had more
to fear from the intrigues of his own colleagues than from
the tactics of the opposition. In 1812 an attempt was
made to form a ministry consisting of men of opposite
political principles, who were invited to accept office, not
avowedly as a coalition Government, but with an offer to
the Whig leaders that their friends should be allowed a
majority of one in the cabinet. This offer was declined
on the plea that to construct a o binet on "a system of
counteraction was inconsistent with the prosecution of any
uniform and beneficial course of policy." From that date
it has been an established principle that all cabinets are to
be formed on some basis of political union agreed upon by,
the members composing the same when they accept office
together. It is now also distinctly understood that the
members of a cabinet are jointly and severally responsible
for each other's acts, and that any attempt to separate
between a particular minister and his colleagues in such
matters is unfair and unconstitutional.
The leading members of an administration constitute the
Cabinet (q.v.). The members of an administration who*
are sworn of the council, but who are not cabinet minis-
ters, are the lord-lieuteuant of Ireland, the vice-president
of the council for education, the judge advocate general,
and the chief officers of the royal hou.sehoid. The sub-
ordinate members of an administration who are never in
the cabinet, and who are seldom raised to the distinction of
privy councillors, are the junior lords of the treasury, the
joint-secretaries to tho treasury, Iho paymaster-general, the
junior lords of the admiralty, the parliamentary under-.'
secretaries of state, and the law officers of tho crown.
During the present century the power of ministers has
been greatly extended, and their duties more distinctly
marked out. Owing to the development of tho system of
parliamentary government, much of the authority which
formerly belonged to English sovereigns has been delegated
to the hands of responsible ministers. As now interpreted,
the leading principles of the British constitution are the
l)ersonal irresponsibility of the sovereign, the responsibility
of ministers, and the iniiuisitorial jiower of jiarliament. At
the head of affairs is the prime minister, and tho difference
between theory and practice is curiously exemplified by
tho post he fills. Tho office is full of anomalies. & Like the
cabinet council the prime minister is unknown _to.tho.laW
VOL . XVI.
M
HORIZONTAL SECTION OF PART OF THE COMSTOCK I
Sfaj^iuetic Xortli
EAST AND WEST SECTION ACROSS F
ilonzoDlaJ .^ Vpi-ijo^
Carbon. uc flill
fla<e U/u. y-OOO ttteh/ibovr ten Ict-ti,
■ Fiuilt '7fiif
pUATEMMAKY
CARHOKUthOrS
fc.al Glarial Jril>
Gla.-iiilLniccb,ds
mo
PL A 'IK [\:
[,331 FEET BELOW THE OUTCROP AT COULD t CURRY MINE
fK*-! Xii I incli.
Explanatiar
.cz
?^ '
D
r OF THE LEADVILLE MINING DISTRICT
Ip ss:t!» 3050 fret = 1 mch
■RIAU
CAJtRRLVN ARCHAEAN
Gramle S? Gneiss
IGNEOUS
White PoiyhTTT Otlierroiplrvriesl
[HI]" [ITj
MINISTRY
473
and the constitutiou, for legally and according to the
fictions of the constitution no one privy counciUcr has as
such any superiority over another, yet practically the
premier is the pivot on which the whole administration
turns. He is the racdium of intercourse between the
cabinet and the sovereign ; he has to be cognizant of
all matters of real importance that take place in the
different departments so as to exercise a controlling
influence in the cabinet; he is virtually responsible for
the disposal of the entire patronage of the crown ; he
selects his colleagues, and by his resignation of office
dissolves the ministry. Yet, though entrusted with this
power, and wielding an almost absolute authority, he
is in theory but the equal of the colleagues he appoints
and whose opposition he can sUence by the threat of dissolu-
tion. The prime minister is nominated by the sovereign.
" I offered," said Sir Robert Peel on his resignation of
office, " no opinion as to the choice of a successor. That
is almost the only act which is the personal act of the
sovereign ; it is for the sovereign to determine in whom
her confidence shall be placed." Yet this selection by the
crown is practically limited. No prime minister could
o.M-ry on the government of the country for any length of
time who did not possess the confidence of the House of
Commons; and royal favour, if it were ever invidiously
exercised, would ultimately have to yield to a regard for
the public interests. As a general rule the prime minister
holds the office of first lord of the treasury, either alone or
in connexion with that of chancellor of the exchequer.
Before 1806 the premiership was occasionally held in
connexion with different other offices, — a secretaryship of
Etate, the privy seal, and the like, — but it is now almost
invariably associated \vith the post of first lord of the
treasury. "" With the exception of the premier, whose duties
fise more general than departmental, the work of the other
members of the administration is exemplified by the title
of the offices to which they are called. The lord chancellor,
in addition to the jurisdiction which he exercises in his
judicial capacity, is prolocutor of the House of Lords by
prescription, the keeper of the sovereign's conscience, the
general guardian of aU infants, idiots, and lunatics, and to
him belongs the appointment of all the justices of the
'peace throughout the kingdom. In former times the lord
chancellor was frequently prime minister ; the earl of
;Clarendon in the reign of Charles II., however, was the
last who occupied that position. The lord president of
the council, who is always a member of the Upper House,
presides over the department of the privy council, exercises
a general superintendence over the education department,
and has to frame minutes of council upon subjects which
do not belong to any other department of state. Sub-
erdinate to his department are separate establishments in
relation to public health, the cattle plague, and quarantine.
The post of lord privy seal is one of great trust, though
its duties are not very onerous, since they simply consist
in applying the privy seal once or twice a week to a
number of patents. Ever since the days of Henry VIII.
the privy seal has been the warrant of the legality of
grants from the crown and the authority of the lord
chancellor for affixing the great seal. The lord privy seal
is always a member of the cabinet. As his official duties
are light he is at liberty to afford assistance to the
administration in other ways, and he has often to attend
to matters which require the investigation of a member
of the Government.
The secretaries of state are among tlie most important members
of the ministry, and within the present century their number has
keen increased and their duties more specially consolidated. The
smcient English monarolis were alwaj's attended by a learned ecclesi-
astic, known at first as their clerk, and afterwards as secretary,
who conducted the royal correspondence : but it was not until the
16— 18»
end of the reign of Queen EUz.ihc th th.it these functionaries were
called secretaries of state. Upon tho direction cf public aflairs
passing from the privy council to the cabinet after 1688, the secre-
taries of state began to assume those high duties which now render
their office one of the most influential ol' au adminLsfration. Until
,the reign of Henry VIII. there was generally only one secretary of
state, but at the end of his reign a second principal secretary was
appointed. Owing to the increase of business consequent upon the
union of Scotland, a third secretary, in 1708, was created, but a'
vacancy occuning in this office in 1746 the third secretaryship was]
dispensed with until 1763, when it was again instituted to take
charge of the increasing colonial business. However, in 1782 the'
office was again abolished, and the charge of the colonies trans-!
fon-ed to the home secretary ; but owing to the war with France in'
1794 a third secretary was once more appointed to superintend the'
business of the war department, and seven years later the colonial
business was attached to his department. In 1854 a fourth secre-
tary of state for the exclusive charge of the war derartment and in
1858 a fifth secretaryship for India were created. There are there-
fore now five principal secretaries of state, four of whom, with their
political imder-secretaries, occupy seats in the House of Commons.
One of these secretaries of state is always a member of the House of
Lords. The secretaries of state are the only authorized eliannels
through which the royal pleasure is signified to any part of the
body politic, and the counter-signature of one of them is necessary
to give validity to the sign manual ; thus, while the personal
immunity of tho sovereign is secured, a responsible adviser for every
act is provided who has to answer for whatever c^^urse the cro^Yn
has pursued. The secretaries of state constitute but one office, and
are coordinate in rank and equal in authority. Each is competent
in general to execute any part of the duties of the secretary of state,
the division of duties being a mere matter of arrangement. The-ie
duties are of the deepest importance to the welfare of tho nation.^
The home secretary conti-ols all matters relating to the internal
affairs of the country : ho is responsible for the preservation of the
public peace and for the security of life and property throughout
the kingdom ; he exercises extensive powers over the civil and
military authorities of the country, and has a direct controlling
power over the administration of justice and police iu the municipal
boroughs, over the police in and around London, and over the
county constabulary ; and he is especially responsible for the exer-
cise of the royal prerogative iu the reprieve or pardon of convicted
ofi'enders or the commutation of their sentences. The foreign secre-
tary, as his name implies, is the official organ of the crown in all
communications between Great Britain and foreign powers : he
negotiates all treaties or alliances with foreign states, protects
British subjects residing abroad, and demands satisfaction for ary
injuries they may sustain at the hands of foreigners. The secretary
of state for the colonies has to superintend the government of the
various colonial_ possessions of the British crown : he appoints the
governors over the different dependencies of the crown, and sane-,
tions or disallows the enactments of the colonial legislatures. This
latter power has of late years been much cui'tailed owing to the
establishment of responsible government in most of the colonie; ;'
still it is the diity of the secretary of the colonies to correspond with'
the colonial governors and to otfer such suggestions as may te^
expedient to assist the deliberations of the colonial councils and to)
promote the welfare of colonial subjects. Until the year 1854 thej
direction of militaiy affairs was practically divided bet^veen the'
commander-in-chief at the horse guards, the board of ordnance, the
secretary at war, and the secretaiy of state for war and the colonies.!
Upon the declaration of hostilities, however, against Russia in 1854,
the duties of war minister were separated from those of colonial!
secretary, and a secretary of state for war appointed, in whose hands'
the supreme and responsible authority over the whole roilitaryj
business of the country formerly transacted by tho various depart-
ments was placed. The actions of the commander-in-chief are sub-
ject to the approval of the secretary of state for war. The duties of
the commander-in-chief embrace the discipline and patronage of the
army and the direct superintendence of the perr^^mel of the army ;
with the exception of those duties, everything connected with the
management of the army in peace or war (its maUricl and civil|
administration, &c, ) remains in the hands of the war minister. Tliel
subordinate position of the commander-in-chief is the result of the'
British system of parliamentary government. The secretary of state
for war is the minister of the crown and not of parliament ; although'
he is responsible to parliament for the advice he may give to tho
sovereign, yet it is in the execution of the royal autliority and
prerogative that he is superior to the officer commanding in chief.!
The principle of the constitutional army is that command, prefer-
ment, and honour come to it from the crown ; but the general prin-
ciple is equally undisputed that for all pecuniary remunerarion it
is made to depend on parliament. By the constitution the crown
exercises its authority only through responsible advisers, and Irenes
it follows that tho secretary of state for war is supremo over any
authority in the army, including the officer commanding in chief.
- From 1781 to 1858 the territories belonging to the British crowniul
474
M I N— M I N
tlic East Indies were governed by a department of state called the
board of control in conjunction with the court of dircctora of the
East India Company. In 1858 this double government was
abolished, and. the entire administration of the British empire in
India was assumed by the crown, and all the powers formerly exer-
cised by tile East India Company and the board of control were
transferred to a fifth principal secretary of state. The secretary for
India is responsible for everything connected with the Indian
Government at home and abroad ; the whole of the Indian revenues
are at his disposal, and the governor-general of India is subject to
his control. To assist him iu his labours, and to act as a check upon
the exercise of liis otherwise arbitrary administrative powers, this
secretary has the aid of a council of state for India, consisting of
fifteen persons, of which, however, he is the president. The members
6t the council for luilia cannot sit iu the House of Commons.
The duties of the other members of the ministry can be briefly
dismissed. The chancellor of the exchequer at present exercises all
the poweis which formerly devolved upon the ti^easury board ; he
has the entire control of all matters relating to the receipt and
expenditure of public money ; be frames the annual estimates of the
sums required to defray the expeuditure of government in every
branch of the public service ; and it is his duty to lay before tho
country the annual statement of the estimated expenses of govern-
ment and of the ways and means by which it is proposed to defray
those charges, including the imposition or remission of taxes. The
lu-st lord of the admiralty {since the abolition of the office of lord
high admiral), with the aid of the junior lords who are called the
lords of the admiralty, conducts the administration of the entire
naval force of the empire both at home and abroad, and is respon-
sible to parliament for all his political proceedings ; as the admiralty
is but an executive board, it is, however, subject on certain matters
— the number of men required for the naval service, the distribution
of the fleet, the strength of foreign squadrons, &c. — to the control
of the cabinet. The president of the board of trade takes cognizance
of all matters relating to trade and commerce, and has to protect
the mercantile interests of the United Kingdom ; until 1864 it was
not necessary for the president to have a seat in the cabinet, but
since that date he has always been a cabinet minister in order to
insure for his advice on commercial matters a duo consideration ; in
3SC7 the office of vice-president of the board was abolished. The
chancellor of the duchy of Lancaster exercises jurisdiction over all
matters of equity relating to lands held of the crown in right of the
duchy of Lancaster ; the office is, however, practically a sinecure,
and is usually filled by a leading statesman whose time is at the
service of the Government for the consideration of such important
rjuestions as do not come within the province of other departments.
In 1832 the public works and buildings of Great Britain were for
the first time placed under the control of a responsible minister of
the crown, and were assigned to the charge of the commissioners of
woods and forests ; but iu 1851 the department of public works was
separated from the woods and forests and erected into a board under
t)ic name of the office of her majesty's works and public buildings.
Tiie fiist commissioner of works is the head of the board, and in his
liquids is placed the custody of the royal jialaces and parks and of all
public buildings not specially assigned to the care of other depart-
ments. Since the establisliinent.of his office the first commissioner
has frequently had a seat in tlie cabinet. The duties of the post-
master-general, of the president of the local govei-nmcut board, and
of the minor members of the administration are so obvious from the
titles of tho offices they hold as not to call for any special mention.
The prime minister is responsible for the distribution of the chief
offices of government bstween tlio two Houses of Parliament.
Owing to the development of the House of Commons within the
present century it is now considered advisable that a larger propor-
tion of cabinet ministers should have scats in that chamber than
was formerly the c.ise.' In the first cabinet of George III. only one
of its membeis was in the House of Commons and thirteen in the
House of Lords. In 1783 Mr Pitt was the sole cabinet minister in
the Commons. In 1801 four cabinet ministei-s were in the Commons
and five in the Lords. In 1804 Mr Pitt and Lord Castlereagh were,
out of a cabinet of twelve, the only ministers in tho Commons. In
tho Grenville ministry ("All the Talents"), of a cabinet of eleven,
seven were in the Lords and four in the Commons. In 1809, of
Mr Perceval's cabinet, six were peers and four commcr.ers. Inl8]2,
of Lord Liverpool's cabinet, ten were peers and only two commoners.
In 1818, out of a cabinet of fourteen, six were commoners ; and in
1822, out of a cabinet of fifteen, nine were peers. Since the' Reform
Act of 1832, however, the leading members of Government have
been more equally apportioned between the two Houses.
Scoilny. Cotitlilulional llhlory of Englntid; C<1X, hiflllulloa, (>/ llm Snyllih
Oovet'nment \ Alpliciu Todd, Ofl ParliaitutUaiy Oovtnimtnt ; Cooke, //istortj of
''"•■'y- (A. C. L.)
MINK. Tlie genus Pntorius, belonging to the family
MusUliilx or Weasel-like animals (see Mammalia, vol.
-\v. p. 440), contains a few species called Minks, distin-
guished from the rest by slight structural modifications, and
especially by semiaquatic habits. They form me suDgenus
Lutreola of Wagner, the genus Vison of Gray. Ab in other
members of the genus, the dental formula is t |, c ^, ^ ;;,
m J ; total 34. They are distinguished from the Polecats,
Stoats, and Weasels, which constitute the remainder of thu
group, by the facial part of the skull being narrower and
more approaching in form that of the Martens, by the pre-
molar teeth (especially the first of the upper jaw) bein^;
larger, by the toes being partially webbed, and by tho
absence of hair in the intervals between the naked pads of
the soles of the feet. The two best-known species, so much
alike in size, form, colour, and habits that although they arc
widely separated geographically some zoologists, question
their specific distinction, are P. lutrcoUi, the l\iir2 or Sumj)f-
otter (Marsh-Otter) of eastern Europe, and P. vison, this
Mink of North America. The former inhabits Finland,
Poland, and tho greater part of Ru.ssia, though not found
east of the Ural mountains. Formciiy it extended west-
ward into central Germany, but it is now very rare, if not
extinct, in that country. The latter is found in placea
which suit its habits throughout the whole of North
America. Another form, P. sihiricus, from eastern Asia,
of which much less is known, appears to connect the true
Minks with the Polecats.
The name may have originated in the Swedish maenh applied
to the European animal. Captain John Smith, in his Hisiory of
Virjjinia (1626), at p. 27, speaks of " Martins, Powlecats, Weesels,
and^llinkes," showing that the animal must at that time have been
distinguished by a vernacular appellation from its congeners. By
later authors, as Lawson (1709) and Pennant (1784), it is often
written "Minx." For the following description, chiefly taken from
the American form (though almost equally applicable to that of
Europe) wo are mainly indebted to Elliott Coues's Fur-lcaring
Animods of North America, 1877. I
In size it much resembles the English Polecat, —the length of the
head and body being usually from 15 to IS inches, that of the tail
to the end of the hair about 9 inches. The female is considerably
smaller than the male. The tail is bushy, but tapering at the end.
The ears are small, low, rounded, and scarcely project beyond the
adjacent fur. The pelage consists of a dense, soft, matted under fur,
mixed with long, stiff, lustrous hairs on all parts of the body and
tail. Tho gloss is greatest on the upper parts ; on the tail the
bristly hairs predominate. Northern specimens have the finest and
most glistening pelage ; in those from southern regions there is less
diflerence between the under and over fur, and the whole pelage ia
coarser and harsher. In colour, dilfcnmt specimens present a con-
siderable lange of variation, but the animal is ordinarily of a rich
dark brown, scarcely or not paler below than on the general upper
parts ; but the back is usually the darkest, and the tail is nearly
black. The under jaw, from the chin about as far back as the
angle of the mouth, is generally white. In the European Mink the
upper lip is also white, but, as this occasionally occurs in American
specimens, it fails as an absolutely distinguishing character. Besides
the white on the chin, there are often other irregular white patches
on the under parts of the body. In very rare instances the tail is
tipped with white. The fur, like that of iiiost of the animals of tho
group to which it belongs, is an inipoi-tant article of commerce.
The piiucipal characteristic of the Mink iu comp.nrison with its
congeners is its amphibious mode of life. It is to the water what
the other Weasels are to the land, or M.irtens to the trees, being as
essentially aquatic in its habits as the Otter, Beavci-, or Musk-rat,
and speniing perhaps more of its time in the water than it does on
land. It swims with most of the body submerged, and dives, with
perfect case, remaining long without coming to the surface to
breathe. It makes its nest in burrows in the bunks of streams,
breeding once a year about the n-.onth of Ajnil, and producing five
or six youn" at a birth. Its food consists of frogs, fish, freshwater
molluscs and crustaceans, as well as mice, rats, musk-rats, rabbits,
and small birds. In common with the other animals of the genus,
it has a very peculiar and disagieeablc clfluvium, which, according
to Cones, is more powerful, penetrating, and lasting than that of
any animal of tho country except tlie Skunk. It also possesses the
courage, ferocity, and tenacity of life of its allies. When token
young, however, it can be readily tamed, and lately Minks have
been cxtcnsiv.ly bred in cijitivily in America both for the sak.- ..f
tlieir fur and fin- the purpose of using them in like manner as Fen irts
in England, to char buildings of rats. (W. H. F.)
MINNEAPOLIS, the county seat of Hennepin county,
Minnesota, United States, and in 1880 the first city of
the State as regards population, lies on both banks of the
t
y
M I N — M I N
47a
Mississippi, at tlie falls of St Anthony, 14 miles by river
abovn St Paul. The east side v/as first settled, under the
name of St Anthony, which was incorporated as a city in
1860. The west side settlement, named Minneapolis, was
incorporated as a city in 1867, and soon surpassed St
Anthony in population. In 1872 the two cities were
united under the name of Minneapolis. The chief in-
dustries are the manufacture of flour and of lumber, for
• |Which the faUs supply abundant water-power. The Missis-
sippi here flows over a limestone bed resting upon a friable
jwhite sandstone; hence erosion is rapid, and the river
banks show that the falls have receded from a position at
ithe mouth of the Minnesota river. In 1851 90 feet of the
limestone gave way at once; and, as the rock bed extends
ibut 1200 feet above the present site of the faUs, the
destruction of the water-power was threatened. This has
been averted by the construction of an apron, or inclined
plane, of timber, with heavy cribwork at the bottom, and
the building of a concrete wall in the bed of sandstone
behind the falls and underneath the channel of the river.
For this work the United States Government appropriated
$550,000 and the citizens of Minneapolis contributed
$334,500. The city has twenty-seven flour-mills, which
can produce 29,272 barrels a day. The total product for
the year ended September 1, 1882, was 2,301,667 barrels.
The shipments of lumber for 1880 were 164,620,000 feet.
^he population in 1870 was 18,079; and in 1880, 46,887.
MIXNESANGER. See Germany, vol. x. p. 525.
to'© MINNESOTA, one of the north-western States of the
American Union, extending from 43° 30' N. lat. to the
British Possessions (about 49° N. lat.), and from Wisconsin
and Lake Superior on the east to Dakota on the west,
between the meridians of 89° 39' and 97° 5' W. long. Its
area, including half of the lakes, straits, and rivers along
its boundaries, except Kainy Lake and Lake of the Woods,
amounts to 83,365 square miles.
The sui-face of Minnesota is diversified by few elevations
of any great height. In general it is an undulating plain,
breaking in some sections into rolling prairie, and traversed
by belts of timber. It has an average elevation above
sea-level of about 1000 feet. The watershed of the north
(which determines the course of the three great continental
river systems) and that of the west are not ridges or hills,
but elevations whoso inclination is almost insensible. The'
southern and central portions of the State are chiefly
rolling prairie, the upper part of which is crossed from
N.W. to S.E. by the forest belt known as the Big Woods, —
a stretch of deciduous forest trees with an area of about
5000 square miles. North of the 47th parallel, the great
Minnesota pine belt reaches from Lake Superior to the
comines of the Red River valley, including the region of
the headwaters of the Mississippi and its upper tributaries,
as well as those of the Superior streams. North of the
pine region there is but a stunjed gro'ivth of tamarack and
dwarf pine. In the north-east are found the rugged ele-
vations of the granite uplift of the shores of Lake Superior,
rising to a considerable height ; while in the north-west
|the surface slopes away to the level prairie reaches of the
Red River valley. The surface elevation of the State
jvaries from 800 to 2000 feet above sea-level. A short line
of hills in the north-east reaches the latter altitude, while
•only the volleys of the Red River, the Mississippi, and the
iMinnesota fall below the former.
Geotogy and Soil. — The geology has not yet been
nnapped out with the precision attained in other States.
jTh« great central zone, from Lake Superior to the south-
Iwestcrn extremity of the State, is occupied by granitic and
metamorphic rocks, succeeded, in the south-east, by nar-
/rower bands of later formation. Within the great Azoic area
Mies the central watijshed of the continent, from which the
St Lawrence system sends its waten towards the Atlantic,-
the Mississippi towards the Gulf of Mexico, and the Red
River of the North to Hudson's Bay. These primordial
rocks carry back the geologic history of Minnesota to pre-
Silurian times. U'hey form in the north-east, in the
neighbourhood of Lake Superior, an extremely rough and
hilly country, but as they reach the central and south-
western portions of the State they for the most part
disappear beneath the surface drift. This central belt is
succeeded, on the south and east, by a stretch of sandstone,
partially the true red Potsdam and partially a similar but
lighter-coloured stratum, which some have proposed to
designate the St Croix Sandstone. Isolated beds of sand-
stone are found in various parts of the State. The north-
western corner, stretching east from the Red River valley,
is believed to be Cretaceous; but the great depth of
drift and alluvium, disturbed by no large rivers, prevents
a positive conclusion. The Lower Magnesian limestone
underlies the extreme south-eastern portion of the State,
and extends along the west side of the Mississippi to a
point a little below St Paul ; thence it takes a course
almost semicircular, and finally passes out of the State at
the south-western boundary. The Trenton limestone
occupies a large field in the south and south-east; it
comes to the surface in long irregular bands, and an island
of it underlies the cities of Minneapolis and St Paul
^vith the adjacent districts. The Galena limestone, the
Masquoketa shales, the Niagara limestone, and the rocks
of the Devonian age in turn prevail in the other counties
of the south and east ; while the existence of the St Peter
sandstone would scarcely be known but for its outcropping
along the bluffs of the Mississippi, and at the famous
waterfall of Minnehaha. From these various formation?
numerous kinds of stone valuable for building jiurposes aro
obtained. The grey granite of St Cloud is extremely hard
and enduring. The Lower Magnesian furnishes two
especially handsome building stones, — the pink limestone
known as Kasota stone, and the cream-coloured stone of
Red Wing, both easily worked, and hardening by exposure
to atmospheric changes. Naturally, from its ^location
underneath the principal cities of the State, the Trenton
limestone is the most widely used. Sand suitable for
glass-making, and argillaceous deposits abound. The
clays which make up so large a portion of the sur-
face drift of the State are almost wholly of glacial
origin. Overlying the deposits of sand, gravel, boulders,
and clay is, in most portions of the State, a sandy
loam, very finely divided, rich in organic matter, deep
bro^^^l or black in colour, and of the greatest fertility.
It is this soil which has given to the State its reputation
for productiveness. Its depth varies from 2 to 5 feet in
various parts of the State, and it has been described by
Dr Owen as " excellent in quality, rich as well in organic
matter as in those mineral salts which give rapidity to the
growth of plants, while it has that durability which enables
it to sustain a long succession of crops."
Rivers and Lakes, — The State holds a unique place with reference
to the great water systems of the continent. The Mississippi takes
its rise in Lake Itasca, north of the centre of the State. Before
it leaves the State limits it becomes a great river, half a mile wide,
and from 5 to 20 feet deep. It drains with its tributaries all
the southern and central portions and a large area of the northern
part of the State. It is navigable as far as St Paul, and at
Minneapolis the falls of St Anthony afford unrivalled facilities
for manufacturing. Of the many affluents of the Mis-
sissippi the most important is the Minnesota, which after a
course of about 440 miles flows into the maiii stream at Fort
Snclling, 3 miles above St Paul. The source of the Minnesota i"
but 1 mile from Lake Traverse, the origin of the Picd Kiver of the
North, and it is navigable during the high-water season for about
238 irules. Its principal tributaries are the Blue Earth, Cliippewa,
Redwood, Lac qui Parle, and Pommo de Terre. Tlie Kcd Rivei
system drains the north-western part of the State, and its vatsy
476
M I N N E S 0 T 'A
finally pass into Hudson's Bay, as also do those from the
country drained by streams flowing to th,e llainy Lake river and
the lakes along the northern boundary line. East of tliis lies the
region tributary to Lake Superior and tlte St Lawrence system.
Tliis comprises an area within the State estimated at 9000 bquare
miles. Its principal river is the St Louis. There mo altogether
about 2796 miles of navigable water in Minnesota.
The number of lakesisestimated at seven thousand. They are of all
sszes, and are found chiefly in the northern tv/o-tliirds of the State.
They have been classified geologically into glacial or drift lakes,
fluviatile or river lakes, occupying basins on river courses, and lakes
having rock basins either scooped out by the action of glaciers or
formed by the rclative-position of different geological formations. By
f«r the greater number give evidence of glacial action in thair origin.
They abound over the region most deeply covered by the surface
drift, and are especially prevalent in morainic districts, forming
the southern fringe of the lacustrine area of North America. With
the melting of the ics-sheet which once overspread Minnesota its
innumerable lakes came into existence ; and the gentle acclivity
of its slopes, precluding rapid erosive action, has terided to give
permanence to the depressions constituting their basins. The
census returns give 4160 square miles of water surface within the
State, Most of the lakes are exceedingly picturesque in their sur-
roundings. Forests skirt their shores, which are seldom marshy ;
and their waters, abounding in various kinds of fish, are clear and
cooL Besides the sanitary advantages afforded by the lakes, as
supplying places for recreation and delightful summer resorts, they
afl^ct the climate to some extent, tempering the extremes com-
monly experienced in northern latitudes. The fact that many of
the lakes are gradually drying up must be explained by agricul-
tural operations. The largest lakes, exclusive of Superior, lying
wholly or in part in Minnesota are as follows : — Lake of the
Woods, 612 square miles ; Ked, 342; Mille Lacs, 198; Leech, I9i;
Rainy, 146; Winuibigoshish, 7S; and Vermilion, 63.
Flora and Fauna. — The flora and fauna present no marked
fUfFei'ences from those of other States in the same latitude. In a
partial list of the birds of ilinnesota, two hundred and eighty-one
species are enumerated. Of winter birds fifty-two species have been
jelassiQed, twenty-three oi them being permanent residents.
Climate. — The State lies so far north as to have a low mean
fennual temperature, and so far inland as to have the characteristic
'oontiueutal climate. Its elevation above sea-level gives an agree-
able rarefaction to the atmosphere, and makes tlie prevalence of
fogs and damp weather unknown. Between Juno and January
there is au annual variation from the summer heat of southern
Ohio to the winter cold of Montreal. The winter, usually com-
mencing in November, and continuing till near the end of ilarch,
78 not a period of intense continued cold, but is subject to consider-
able variations. As a rule, the comparative dr3'uess of the atmo-
sphere neutralizes the severest effect of excessive cold. The snowfall
is extremely light during most of the winter, but as spring
approaches precipitation becomes greater, and there are frequently
heavy snowfalls in February and March. The change from winter
to summer is rapid, vegetation sometimes seeming to leap into full
and active growth within the space of a few weeks. The summer
months bring days of intense heat, but, with comparatively rare
exceptions, the nights are delicinusly cooL Hot days and cool
Bights make the ideal weather for a good wheat crop ; and the
forcing heats of summer produce in luxuriant growth the vegetable
life which belongs to the middle States. Tlie Smithsonian chart
assigns to Minnesota an average temperature for the hottest week
in summer of from 85° to 90", and for the coldest .vcek in winter
from 10° to 20'' below zero. The moan annual average, for all
below 47° of latitude, it gives as 40^ Observations at St Paul,
extending over a period of more than thirty-five years, show the
following mean temperatures: — spring, 45''"6 ; summer, 70°"6 ;
autumn, 40'-9 ; winter, 16"-1 ; average, 44*-6. The average annual
rainfall is about 25 '5 iuches. While this is not large, it is so
distributed as best to subserve the purposes o? vegetable growth.
No moisture is lost in superfluous spring and autumn rains, or in
the cold and non-producing part of the year, tJie precipitation, whicli
in winter is less than 2 inches, increasing to about 12 for the sum-
mer. To the season of vegetable growth belong 70 per cent, of the
yearly measures of heat, 76 percent, of the rainfidl, and 76 percent,
of the atmospheric humidity. The prevailing winds are from the
wntli or south-east. In 1880 rain or snow fell on 150 days, and in
1881 on 167. It is evident that the causes which mitigate the actual
severity of the climate as felt, which produce so large a number of
clear dap, and which forbid the continued presence of a large amount
of mois'turo in the atmosphere, aro those which ren<ler a climate
hoaltiiful in the highest degree, Minnesota has been for many
years a favourite resort for invalids. The curative properties of its
cUmste are especially marked in the case of pulmonary complaints.
AgricuHure. — The leading industry of the State is agriculture.
The character of the surface soil varies in diflerent parts of the
State with the character of the underlying strata. The fertile lond
•qanprises about tliree-foui'tha of the eutiro area of the State. The
drift soil proper of the south and centre, including the MinncaQfir
valley and the greater part of that of the Mississippi, contains silic*
and calcareous matter, and is interspersed with alluvial rivti
bottora.s. The liuicotone soil, in which there is a large calcareou*
element, lies chiefly on the western slope of the Mississippi. Th«
Ked River valley consists of an argillaceous mould, rich in organic
deposits. Around Lake Superior, wherever arable land is to hi
found, it is marked by a rich trap soil. North of the central fertih
area, and in the neighbourhood of the sources of the Mississippi, ij
much swampy land, susceptible of ea^y drainage, with a largo trad
of sand and other drift detritus, unfavourable to production. Mair"-
and potatoes flourish, and the uplands, which support hardwood
ridges, are suited to general agriculture. To the extreme ncrtli
the surface, while indicating mineral wealth, is utterly un6t, e:;ctpi
in occasional isolated areas^ for purposes of tillage.
Wheat has hitherto been the staple product of the State. Soil
and climate are such as to ensure a large average yield, while the
superior quality of the grain has given it a wide reputation. Tlie
otb.er cereals are also cultivated wit!i success. The tendency to
diversify agriculture, especially in the southern part of the Slate,
has been stimulated by several partial failures of the wheat crop,
the locust invasions, and the competition of the farther north-west.
The area of the State includes 39,791,265 acres surveyed,
10,968,575 acres not sun'eyed, and 2,700,000 acres of lake surface.
Thetotalsalesof public and railroad lands in 1879 and 1880 were not
far from 4,000,000 acres. It is estimated that the aggregate oi
lands yet undisposed of, three-fourths of which may be prof]^ably
cultivated, is nearly 20,000,000 acres, exclusive of the lands belong-
ing to the State. White Earth Indian reservation has thirty-six
townships of prairie and timber land ; and Red Lake reservation
contains 3,200,000 acres.
Forestry. — A special census bulletin estimates the amount ol
merchantable white pine standing. May 31, 1880, as amounting in
all to 6,100,000,000 feet. The entire cut for the census year 1880
was 540,997,000 feet. Of hardwood forest 3,840,000 acres remain,
capable of yielding 57,600,000 cords of wood.
Every encouragement is afforded, both by the railway coi-pora-
tions and the State, to tree-idanting on the prairies. A quarter
section is given to any one who will plant and keep in good condi*
tion 40 acres of timber for eight years. In ISSO there were planted
25,331 acres of trees, exclusive of those bordering highways and
the windbreaks along the railroad lines.
Manufactures. — The manufactures of Slinnesota are yet in their
infancy. The abundant water-power of the State, its proximity to
the coal-fields of Iowa, its superior transportation facilities, and the
large demand for manufactured commodities are, however, rapidly
developing this branch of industry. The most important industries
are the manufacture of flour and t^iat of lumber. The former natu-
rally established itself in aState of immense wheat yield and abundant
water-power. It received its greatest stimulus from the invention
and adoption of the middlings purifying process, which produces
the highest grade of flour, and to which the hard spring wheat of
Minnesota is especially adapted. Among other manufacturing
industries actively prosecuted are the makin^ of brick, pottcrj",
stoneware, and agricultural implements, and also meat-packiug.
Commerce. — The geographical position of Jlinncsota gives it ex-
tensive commercial interests. Two continental waterways tcrmiuutc
within the State. The Mississippi affords continuous navigation
to European jwrts during eight months of the ye.-.r. From Duluth
numerous lines of vessels traverse the chain of great lakes, nud,
transport the products of the west to the eastern seaboard. Tlirce
great transcontinental railway lines are connected more or less
directly with the railroad system of the State. Twelve lines of rail-
way from every part of Minnesota converge at the contiguous cities
of St Paul and Minneapolis, and three great trunk lines from thes«
centres to Chicago secure the advantages of a lively competition.
Education. — The common school system is supported by land
grants, a local tax, and a State tKX. The superintendent of in-
struction is appointed by the governor. County superintendents
aro chosen by popular vote. Common school districts have boards
of three trustees each. Six directors are ajipointed for indeiiendeut
districts. The permanent fund in 1881 was §4,850,000, am\ the
current fund $260,835. The State university, located at Minnea-
polis, is governed by a board of regents, consisting of the governor
of the State, the superintendent of public instruction, the president
of tlie university, and six others ; both sexes aro admitted, and
tuition is free. The State supports three normal schools. Forty-
two academies and six colleges are sustained by denominational or
private enterprise.
Administration. — The departments of Government are, as in all
the States, tlie legislative, tlie executive, and the judicial. The
State contains seventy-eight counties, of which some are still
subject to change of boundary. From these nre elected by district*
forty-seven senators and one hundred and three members of the
House of Representatives. The State officers arc a governor,
lieutenant-governor. Recretary of state, treasurer, and nttorney-
gencral, all elected by the t)Oople. The term of oflfice is two yeara.
M I N — M I N
477
ThP governor has power to veto separate items of a money bill The
judiciary is elective, and the term of ofDce seven years. The State
i-cquirements for citizenship are residence in the United States
one year, in the State four months, and in the election district
tci) days preceding an election. Women are allowed to vote for
school omcers and upon questions relating to the management of
sciiools, and are also eligible to such offices. No county can con-
tain more than 400 square miles. The legislature meets biennially.
Extra sessions may be called, but uo session can exceed sixty days
in length. Under the last apportionment the State is entitled to
live representatives in the national Congress.
The annual valuation of property for 18S2, as equalized by the
State board, gives the personal property as $79,219,445, the real
estate $242,938,170. This represents a total actual value of not far
from S75O,O0O,O_00.
While Minnesota \,-aa still a Territory, but after it had adopted
a State constitution, an amendment was added to the constitution
authorizing the issue of a large amount of bonds in aid of railway
construction. Shortly afterwards, the companies having failed to
fulfil their contracts and defaulted payment, tl\e State foreclosed
its mortgage oa tlio lands, f i"auchises, kc , of the roads, and turned
them over to other companies. By another amendment to the
constitution, the payment of the bonds was made contingent ujpon
the rfesult of a popular vote. Several proposals having failed to
receive this sanction, the necessity for it was removed in 1881 by a
decision of the supreme court, declaring the amendment uncon-
stitutional. The legislature immediately met, accepted a plan of
settlement proposed by the bondholders themselves, and over
94,000,000 worth of new bonds were issued in exchange for the old.
For the payment of the principal and interest of these the people
have voted (November 1882) to set aside as a sinking fund the
proceeds of 500,000 acres of land belonging to the State internal
improvement fund, the deficit to be paid out of the tax on railroad
e,iniiugs. The.se bonds include all the State debt except about
3200,000. A tax of 3 per cent, imposed on the gross earnings of
all railroads within the State will soon meet all expenses except
provision for educational, penal, and charitable iiistitutions.
Populalioii. — T\\i poimlation of the State was 6077 at the census
ofl850, 172,023 in 1860, 439,706 in 1870, and 780,773(419,149
males and 361,624 females) in 1880. According to the last census
299,800 whites had been bovn in the State; and of the 267,676
foreign-born iuhabitauts of the State 107,770 came from Scandina-
vian countries and 68, 277 from the United Kingdom and the British
colonies, while 77,505 acknowledge the German as their native
tongue. The increase of population in the State for the last decade
of yeai-s alone was 75 per cent. The most important cities are St
Paul, the capital, and Minneapolis, with 41,473 and 46,887 inhabit-
ants respectively in 1880; Winona had 10,208 and Stillwater 9055.
History. — Missionary efforts and the trading spirit fii-st induced
white men to venture as far into the unexplored north-west as the
boundaries of what is now the State of Minnesota. The earliest
accounts of its natural features and native tribes appear in the
Jesuit writings. The "Relations" of 1670-71 allude to the Sioux
ovDakotas. In 1678 a company was formed for trading with this
tribe. Du Luth was leader of this expedition, and later on went
fi-om Lake Snpeiior to the Mississippi by canoe. But the first pub-
lished account is that of Louis Heunepiu, a Recollect monk, who,
in 1680, visited the falls of St Anthony, and gave them their name,
from that of his patron saint. For a century the only visitants
of the wild region were a few missionaries, and a number of fur
ti-aders who found the profit of the journey to more than counter-
balance its perils and hardships. To the latter class belong PeiTOt,
who reached the Mississippi by way of the Fox and Wisconsin in
1684, and founded at Lake Pepin the first trading post in the State,
and Le Sueur, a Canadian, who ascended the gi'eat river from its
mouth, and established another post above Lake Pepin. Captain
John Carver, the explorer of the country of the upper Mississippi,
visited the falls of St Anthony in 1766, being the hrst British tra-
veller who reached the spot. On March 20, 1804, Upper Louisiana
was organized, consisting of Arkansas, Missouri, Iowa, and a large
portion of Minnesota. From this time onwards the progress of explo-
ration was rapid, and settlement followed in its tr,ain. The first
really extensive exploration of any large part of what is now
Minnesota was made between 1817 and 1823, by Major S. H. Long,
of the United States engineer corps, in command of a Government
expedition. About the same time the Red River received its fii-st
visitant Thomas Douglas, earl of Selkirk, an Englishman of
eccentric character, went, in 1817, to what is now Winnipeg, by
w.iy of York river. Having been struck with the agricultural
possibilities of the region about the Red River of the North, he
, induced a colony of Swiss farmers to settle there. Thee were dis-
appointed in the country, and unused to the severity of the climate,
so that they finally removed to the vicinity of St Paul and con-
tributed to the earliest development of the agricultural in-
dustry of the State. In 1821 Colonel Snelling built, at the
junction of the ifinnesota and MLiisissippi rivers, a stronghold
which he nonied Fort St Anthony. The name was changed to Fort ,
SncUing in his honour, in 1824, and the fort is still an important
post as a b.ise of si-pplies for the newer north-west The fin*
steamboat made its appearance at the head of navigation in 1823.
The settlement of St Paul, one of the oldest towns as well as th«
capital, is commonly dated from 1 846, at which time there were a few
shanties on its site. Population now began to a:Tive in constantly
increasing numbers, and on March 3, 1849, a bill passed Congress foe
organizing the Territory. It was proposed at one time to name it
Itasca, but the name Minnesota, meaning, "sky-tinted water,"
and originally applied to the river bearing that title, was fmtily
retained. The western boundary of the territory was fixed at th«
Missouri river. The population was but 4057, the largest town
had but a few hundred inhabitants, and a large part of the soil of
the State still belonged to the Indians. But progress now began in
earnest. A constitution was adopted in 1857, and on May 11, 1858,
Minnesota was admitted as a State, with a population, according
to the last Territorial census, of 150,037.
One of the first acts of the new State was the issue of the rail-
road bonds noticed above. Soon after came the civil war. Within
two months of Lincoln's first call for troops the first Minnesota
regiment, over one thousand strong, was mustei-ed into service. By
August of 1862 ten regiments had been called for and furnished. la
all, the State supplied to the armies of tlieUnion 25,052 men, or about
one-seventh of its entire population at the outbreak of the war.
In the meantime there occurred, in 1862, the horrible outbreak
known as the Sioux massacre. Settlements were cut off, isolated
settlers murdered, and even a strong post like Fort Ridgely was
attacked. The outbreak spread over a large portion of the State;
several severe engagements were fought ; and it was not until the
State had a thoroughly equipped military force ready for the cam-
paign that the Indians begun to flee or to give themselves up. By
this time over 700 persons had been murdered, 200, chiefly women,
taken captive ; eighteen counties were ravaged, and 30,000 people
were homeless. Ihe property loss was not less than $3,000,000.
During these local and national disturbances the matei"ial pro-
sperity ot the State was unabated. Notwithstanding the heavy cost
of the civil war and the Sioux massacre, the census of 1865 showed
a population of 250,099. Railroad construction began to be ener-
getically carried forward ; in 1870 329 miles were made and lOttf
miles were in operation ; a road to Lake Superior was completed,
and the Northern Pacific was fairly under way. In 1873-76, and
to some extent in 1877, successive visitations of locusts destroyed
the crops of the south-western counties. The sufferers wens
relieved by the Stat,e, and no repetition of the scourge has since been
experienced. (J. G. P.)
MINNOW (Leuciscu3 plioximn or Phoxinus Ixvis) is the
smallest British Cyprinoid, readily distinguished by its
very small scales. It is abundant in rivers, brooks, and
lakes, always swimming in schools, and shifting its ground
in search of food, which consists of every kind of vegetable
and animal substance. It ranges from southern Euroiie
to Scandinavia, and from Ireland into north-eastern Asia ;
in the Aljis it attains to a higher altitude than any other
Cyprinoid, viz., to ffearly 8000 feet. Its usual size varies
between 2 and 3 inches ; but in suitable localities, especially
in Germany, it is known to reach a length of from 4 to 5
inches. The colours varj- with age and season ; a series of
dark spots or cross-bands along the sides is always present,
but the males assume in summer a nuptial dress of scarlet
or pvirple on the lower parts of the head and body.
The minnow is used as bait ; it can also be introduced
with facility and with great advantage into ponds in which
there is otherwise a scarcity of food for more valuable
fishes, such as trout, perch, and pike.
MINO DI GIOVANNI (1431-1486), caUed da Fiesole,
was bom at Poppi in the Casentino in 1431. He had
property at Fiesole, whence his usual name. Vasari'a
account of him is very inaccurate and full of contradictions.
Mino was a friend and fellow-worker both with D. da
Settignano and Matteo Civitale, all three being about the
same age. There is considerable similarity in their works,
showing mutual influence. Mino's sculpture is remarkable
for its gem-like finish and extreme delicacy of detail, as
■well as for its spirituality and strong devotional feeling.
No other sculptor portrayed the virginal purity of the
Madonna or the soft infant beauty of the Divine Child with
greater tenderness and refinement. Of Mino's earlier
ivorks. the finest are in the duomo of Fiesole, the altarpiece
478
M I N — ]\i 1 :n.
and tomb of Bishop Salutati, executed abotit 1464. In
the Badia of Florence are some of Mino's most important
sculptures — an altarpiece, and the tombs of Bernardo
Giugni, 1466, and the Margrave Hugo, 1481 — all sculp-
tured in white marble, with beaiitiful life-sized recumbent
eflSgies and attendant angels. The pulpit in Prato
cathedral, finished in 1473, is very delicately scidptured,
,with bas-reliefs of great minuteness, but somewhat weakly
designed. Soon after the completion of this work Mino
Eid a visit of some years to Rome, where he executed
feral fine pieces of sculpture, such as the tomb of Pope
,ul IL (now in the crj^Jt of St Peter's), the tomb of
I"rancesco Tornabuoni in S. Maria Sopra jlinerva, and a
jbeautiful little marble tabernacle for the holy oils in
6. Maria in Trastevere. There can be little doubt that he
was also the sculptor of several of the very lovely monu-
ments in S. Maria del Popolo, especially those in the
sacristy of Bishop Gomiel and Archbishop Kocca, 1482,
and the marble reredos, also in the sacristy, given by Pope
Alexander VL Some of Mino's portrait busts and delicate
profile bas-reliefs are preserved in the Bargello at Florence ;
they are full of life and expression, though without the
ejrtreme realism of Verrocchio and other sculptors of his
time. He died in 1486.
See Tasari, Milanesi's ed., 1878-82; Peikino, Italian Smtpiors;
WiQckelmaun and D'Agincourt, Storia delta ScuUura, 1813.
MINOR. See Infant.
MINORCA. See Baleaeic Islands.
MINORITES. See Feakmscajjb.
MINOS, a legendary king of Crete, in whom both
historical and religious elements are united. The historical
element lies in the fact that an early civilization and mari-
time power had its seat in Crete. The Phojnician inter-
com-se played a great part in developing this island state,
and Minos is sometimes called a Phoenician. The name Minoa
is often found where Phojnician influence was strongest,
e.ff., at Megara. The laws and constitution which existed
from a very early time in Crete were attributed to Minos,
to whom they were revealed by Zeus. After his death he
became the judge of the dead ; he is one of the forms
assumed by the old conception of the first man, who is
after death king and god among the dead. It is therefore
highly probable that the name Minos is the Greek form of
the original Manva, i.e., " endowed with thinking," which
is seen in the Hindu Manu and the Germanic Mann. As
in all other heroized forms of the god of the dead, there
is both a terrible and a wise and beneficent side in the
character of Minos. Cretan legends described him as the
Avild huntsman of the fore.sts and mountains, the lover of
the nymphs, though his love means death to them. His
death is localized in the far west, in the land of sunset ;
his grave was shown at Camicus near Agrigentum, attached
to a temple of Aphrodite. He pursued Diedalus thither,
and the daughters of Cocalus, the king of Agrigentum,
killed him by pouring boiling water over him in the bath,
au obvious mj-th of the sun dying in the sea. Jlinos, the
god of the dead, is, according to the usual nU», the sun-god,
who goes to illumine the dead when he dies on the earth.
His wife is Pasiphae, the moon-goddess, who had an oracle
by dreams at Thalamre in Laconia. The union of the sun
and the moon, the buU and the cow, gave rise to many
quaint and ugly legend.^ : Pasiphae loved the buU of Minos,
was aided by the stratagem of Daedalus, and gave birth to
the Minotaur, half bull and half man. The Minotaur is
one of those monstrous forms which were suggested to the
•Gfreek fancy by the quaint animals .common in Oriental
t)rt. It was shut up in the L.vbvrittii (7.I.), which was
•■onstructed by the skilled artist Dicdalus. Now a son of
Min^s named Androgens had been killed by the Athenians,
*nd.Minos as a punishment required that seven Athenian
youths and seven maidens should be sent every ninth year
and given up to the Minotaur to be devoured. When this
sacrifice took place for the third time Theseus came as one
of the hostages, and slew the Minotaur with the help of
Ariadne. Throughout these legends we see the close
relation of Minos to the Phanician sun-god Melkarthj and
perceive the way in which different places where Phoenician
influence can be traced, Athens, Sicily, ic, are brought
together in religious m}'ths.
MINOTAUR. See Minos.
MINSK, a western government of Russia, is bounded
by Vilna, Vitebsk, and MoghilefE on the N. and E., and
by Tchernigoff, Kicff, Volhynia, and Grodno on the S.
and W., and has an area of 35,175 square miles. The
surface is undulatmg and hilly in the north-west, where a
naiTov/ plateau and a range of hills of the Tertiary forma-
tion runs to the north-east, separating the ba.sin of the
Niemen, which flows into the Baltic, from that of the
Dnieper, which sends its waters into the Black Sea. The
range, which averages from 800 to 1000 feet, culminates in
Lysaya Gora (1129 feet). The remainder of the province
is flat, 450 to 650 feet above the sea-level, covered with
sands and clays of the glacial and post-glacial periods. Two
broad shallow depressions, drained by the Berezina and the
Pripet, cross the province froui north to south and from
west to east; and these, as well as the triangular space
between them, are covered with immense marshes (oi'teti
occupying 200 to 600 square miles), numberless ponds ar.d
small lakes, peat-bogs, downs, and moving sands, as well
as with dense forests. This country, and especially its
south-western part, is usually known under the name of
Polyesie (" The Woods "). Altogether, marshes take up
15 per cent, and marshy forests no less than 55 per cent,
of the entire area of the province (60 to 71 per cent, in
several districts). The forests, however, consist cf full-
grown trees in the higher districts of the north- v\ st
only, those which occupy the marshy ground consisting 'A
small and stunted pine, birch, and aspen. The climate of
the Polyesie is harsh and extremely unhealthy ; malarias
and an endemic disease of the bulbs of the hair {koltir.i,
plica Polonica) are the plagues of these tracts, the evil
being intensified by the dreadful poverty of the popula-
tion. Communication is very difficult. The railway from
Poland to Moscow has, so far asJMinsk is concerned, taken
advantage of the plateau above mentioned ; but still it has
to cross the broad marshy depression of the Berezina. A
successful attempt was recently made to drain the mar.-hes
of the Polyesie by a system of canals, and more than
4,500,000 acres have thus been rendered suitable for patture
and agi'icidture. Txvo great tributaries of the Dnieper, the
Berezina and the Pripet, both navigable, with numberless
subtributaries, many of which are also navigable, are the
natural outlets for the marshes of the province. The
Dnieper flows along its south-eastern border for 160 miles,
and the Niemen on the north-western for 130 miles. The
affluents of the Baltic, the Duna (Dwina), and the Vistula arc
connected by three canals with tributaries of the Dnieper.
The population of the province (1.183,200 in 1873) may
be estimated at about 1,350,060, mostly A\Tiite Russians
(67 per cent.); there are also Poles (about 11 per cent.),
especially in the western districts, Jews (more than 10
per cent.), Little Russians (5 per cent.), and Russians (2 jicr
cent.). About 70,000 are considered to bo Lithuanians ;
there are also 4000 Tartars, whose presence can be ti.iojd
to the raids of their ancestors on Litnuania in the liUli
century, and about 2000 German agriculturists who settled
in last century
The chief occupation of the inhabitants is agriculture, which is,
however, verv unjiroihictive in tlic lowlands ; in tho Polyesie the
peasants rarely ha\'o pure licad to cat. Only 23 '8 i>cr cent, of tli'.
M I N — M I N
479
»rea is tmJrt wops, the arerago yield being 1,600,000 qnartcrs of
com and 1,170,000 quarters ot potatoes. Cattlebrecdiug is very
imperfectly developed, the meadows being marehy throughout the
lowlands. Hunting and bee-keeping are sources of income iu the
Polyesie, and fialiing gives occui)atioii to about twenty thousand
persons. The chief source^f Income for the inhabitants of tho low-
lands is the timber trade. Timber is floated down the rivers, and
tar, pitch, various products of bark, potash, charcoal, and numerous
eorts of timber- ware (wooden dishes, tc. ) are manufactured in villages
to a gieat extent ; and shipbuilding is carried on along tho Dnieper,
Pripet, and Niomen. Shipping is also an important source of
income, owing to the traffic on the canals and rivers of the province.
In 1877 5G0 boats and 1120 rafts with 170,000 m-ts. of cargo left
the banlis of the Berezina and Pripet ; and the traffic on the Dnieper
and Niemen was nearly as gi-eat. The industrial arts are almost
entirely undeveloped. There are, however, several distilleries and
tanneries ; and woollen-stuffs, candles, tobacco, and sugar are manu-
factured to a limited extent. Com is exported from the western
districts, but imported to the same amount into the southern parts ;
the chief export trade is in produce of forest industries. The pro-
vince is crossed by two important railways, one of which connects
Poland with Moscow, an(f the other Libau and Vilna with the
provinces of i,ittle Russia; the great highway from Warsaw to
Moscow crosses the province ill the south, and its passage through
tho Berezina is protected by the fiist-class fortress of Bobruisk.
Minsk is divided into nine districts, of which the capitals are —
Minsk(43,S0O inhabitants), Bobruisk (26,850), Borisoff(5650), close
by the place where Napoleon I. crossed the Berezina on his retreat
from Moscow, Igumcn (2200), JilozjT (42001, Novogrodek (9000),
Pinsk (18,000), Ryechitea (4300), and Slutsk (17,200). Tho pro-
vince is well provided with secondary schools, but primary edu-
tation, especially in the Polyesie, is in a very backward state.
Tho country now occupied by the province of Ihliijsk was, as far
as historical records extend, an abode of Slavonians. That portion
of it which was occupied by the Krivichi became part of the Polotsk
principality and so of " White Russia" ; the other portion, occu-
pied by the Dregoviclu and Drevlans, became part of the *' Black
Russia " ; whilst the south-western portion of it was occupied by
Yatvyags or Litliuanians. Duiiiig the 12th, 13th, and 14tli cen-
turies it was divi<lcd among several pvineip.alities, which were in-
corporated with the great principality of Lithuania, and later were
annexed to Poland. Russia took possession of this country iu
1793. Ill 1812 it was invaded by the army of Napoleon I.
Minsk, the capital of the above province, is situated
0-1 the Svislocb, a tributary of the Berezina, at the
junction of tlie JIoscow and AVarsaw and the Libau
and KharkofE railways, 465 miles by rail west from
Moscow. It has 43,500 inhabitants, of whom one-third
are Jews of the poorest class; the others are AVhite
Russians, Polos, and Tartars (about 700). The manufac-
tures are few and insignificant. Since the introduction of
railways the commercial importance of the place, which
formerly was slight, has begun to increase.
Minsk is mentioned in Russian annals in the 11th century under
the name of Jlycn'sk or Jlenesk. In 1066 and 109C it was dovas-
(ated, first by Izyaslav and afterwards by Vladimir. It changed
mlcra many times until the 13th century, when it became a Litliu-
aiiiaii fief. In the 15th century it became part of Poland, but as late
as 1505 it was ravaged by Tartars, and in 1508 by Russians. In the
1 8th century it was taken several times by Swedes and Russians.
Russia annexed it in 1793. Napoleon I. took it in 1812.
MINSTREL. The "minstrels," according to Bishop
Percy, " were an order of men in the Middle Ages who
united the arts of poetry and music, and sang verses to the
harp of their own composing, who appear to have accom-
panied their songs with mimicry and action, and to have
practised such various means of diverting as were much
admired in those rude times, and supplied the want of more
refined entertainments." This conception of the "minstrel " .
has been generally accepted in England ever since Percy
published his Seli'iues of Aiirient Foelry, which he gave to
the world as the products of the genius of these anonymous '
popular poets and harpers. The name has been fixed in
the language by the usage of romantic poets and novelists ; j
• Scott's "last minstrel" and Moore's "minstrel boy" were
minstrels in Percy's sense of the word. The imagination I
was fascinated by this romantic figure, and the laborious
and soured antiquary Eitson argued in vain that nobody
b«fore Bishop Percy had ever applied the word minstrel to I
euch an order of men, that no such order of men e\er did '
exist in medieeval England, and that the historical English
" minstrels," so-called, were a much less gifted and respect-
able class, being really instrumental musicians, either
retainers or strollers.
The dispute between Ritson and Percy was partly a dis-
pute about a word, and partly a dispute about historical
facts; and there can be little doubt that Ritson was substan-
tially right in both respects. The romantic bishop trans-
ferred to the mediaeval English minstrel the social status
and brilliant gifts of the Anglo;Saxon gleoman or scop, and
the French troubadour in the flourishing period of Proven9al
poetry. Thatthegleemen sang tDthe harpversesof their own
composing, that some of them travelled from court to court
as honoured guests, while others were important attached
court officials, and all received costly presents, is a well
attested historical fact. The household bard at Heorot in
the poem of Beowulf, a man who bore many things in mind
and found skilfully linked words to express them, was one
of King Hrothgar's thanes ; the gleeman of the Traveller't
Song had visited all the tribal chiefs of Europe, and received
many precious gifts, rings and bracelets of gold. The
incidents in these poems may not be historic, but they
furnish indubitable testimony to the social position of the
gleeman in those days ; a successful gleeman was as much
honoured as a modern poet-laureate, and as richly rewarded
as a fashionable prima donna. Further, the strolling glee-
man of a humbler class seems to have been respected as a
non-combatant; this much we may infer from the stories
about Alfred and AnlaS having penetrated an enemy's
camp in the disguise of gleemen, whether these stories are
true or not, for otherwise they would not have beea
invented. The position of poets and singers in Provenco
from the 11th to the 13th century i.s still clearer. The
classification of them by King Alphonso of Castile in 1273,
by which time honourable designations were getting mixed,
may help to determine the exact position of the English
"minstrel." There was first the lowest class, the Oufos,
who strolled among the common people, singing ribald
songs, playing on instruments, showing feats of skill and
strength, e.xhibiting learned dogs and goats, and so forth ;
then the joc/lars or jocufatores, who played, sang, recited,
conjured, men of versatile powers of entertainment, who
performed at the houses of the nobility, and were liberally
remunerated ; then the irohadors, or inventores, whose dis-
tinction it was to compose verses, whether or not they had
sufficient executive facidty to sing or recite them.
If we compare these distinctions with Percy's definition
of the minstrel, we see that his minstrel would have corre-
sponded with the jor/lar, who also wrote his own songs and
recitations. Now in the palmy days of Provencal scng
there were many professional joglars, such as Arnaut
Daniel or Perdigo, who stood high among the most brilliant
troubadours, and visited on terms of social equality with
nobles and princes. But long before Englisli became the
court language the fashion had disappeared, and a new
division of functions had been developed. In Chaucer's
time the poet of society no longer sang his verses to harp
or fiddle, or amused his patrons witli feats of legerdemain ;
the king's r/eslour (teller of tfes/rs) discharged tlie profes-
sional duty of amusing with witty stories ; and the social
position of the Joylar had very much sunk. Ritson \vas
perfectly right in saying that no English poet of any social
position was a professional reciter to the harp of verses of
his own composing. The Provenij-al joglar, travelling from
court to court, combined our modern functions of poet,
society journalist, entertainer, and musician. But about
the time when the word " minstrel " came to be applied to
him the English joglar was rapidly sinking or had already
sunk to the social position of the modern strolling mounte-
bank, travelling showman, or music-liall singer. • Aad the
480
M I N— M I N
word minstrel had had a sepamte history before it became
synonymous (as in the Calholicon Atifflimm of 1483) with
ge^icviator, kistrio, joculator, and other names for strolling
entertainers. Derived from the Low Latin ministralis, it
was originally applied to those retainers whose business it
was to play upon musical instruments for the entertainment
of their lords. Li Chaucer's Squire's Tale, the " minstralles "
play before King Cambuscan as he dines in state " biforn
him at the bord deliciously," and the " loude minstralcye "
precedes him when he rises and withdraws to the orna-
mented chamber,
TUer 03 they somicu diuerse instrumentz,
That it is lyk nu heuen for to hen
Bat even in Chaucer's time there were less respectable
musicians than those of the king's household — strolling
nuisicians, players on trumpets, clarions, taborets, lutes,
rebecks, fiddles, and other instniments. These also were
known by the generic name of minstrels, whether because
many of them had learnt their art in noble households
before they took to a vagabond lite, or because the more
respectable of them affected to be in the service or under
the patronage of powerful nobles, as later on companies of
strolling players figured as the " servants " of distinguished
patrons. All the allusions to minstrels in literature from
Langland's time to Spenser's point to them as strolling
musicians. Some of them may have sung to the harp
verses of their own composing, and some of them may have
composed some of the ballads that now charm us with their
fresh and simple art ; but the profession of the "minstrel,"
properly so-called, was much less romantic than Bishop
Percy painted it. It was not merely " the bigots of the
iron time " that " called their harmless art a crime "; in a
repressive Act passed by Henry IV. they appear with
" westom's, rymours, et autres vacabondes " among the
turbulent elements of the community.
In a passage in Malory's Morte Darlhur, the word
inirLstrel is applied to a personage who comes much nearer
the ideal of the PrOT'en9al joglar. When Sir Dinadau
wished to infuriate King Mark, he composed a satirical
song, and gave it to Elyot a harper to sing through the
country, Tristram guaranteeing him against the conse-
quences. ^Yhen King Mark took him to task for this, the
harper's answer was, " Wit you wtU I am a minstrel, and
I nmst do as I am commanded of these lords that I bear
the arms of." And because he was a minstrel King Mark
allowed him to go imharmed. The service done by Elyot
the harper in the old romance is a good illustration of the
[Kjlitical function of the itinerant vieAixvaXjoculator; but
even he did not sing verses of his ovra composing, and he
was not a " minstrel " in the sense in which the word was
used by romantic poets after the publication of Percy's
Religues. (w. m.)
MINT. The mint is the place where the coinage of a
country is manufactured, and whence it is issued by sovereign
nuthority, under special conditions and regulations. The
j)rlvilege of coining has in all ages and countries belonged
to the sovereign, and has, in England at least, been rarely
delegated to any subject, and in any case in a restricted
form, the crown always reserving the right of determining
the standard, denomination, and design of the coins.
At a very early stage of civilization it was found
necessary to have some definite medium of exchange, in
crder to avoid the great inconvenience arising from the
bystem of payment in kind, which was the primitive and
•n.tural method. It was not long before metal came to be
: 36d as such a medium, probably from its duiability and
, ortability, and in the case of gold and silver on account of
tiieir intrinsic value. The less liable the value of a metal
: . to change the better is it suited for a standard of value.
Though historians assure us that metals were found in
Britain at a very e^ily period, there does not appear to be
any evidence that the mines were worked imtil consider-
ably later than the time at which the use of metal as a
medium of exchange v.as introduced. It is probable there-
fore that the metals for exchange were imported into
Britain long before the native mines were developed.
The metals chiefly used were silver and brass, which
were at first simply exchanged by weight for commodities
of all kinds. As commercial transactions became mora
numerous and more complicated, this system of payment
grew troublesome, and it was found convenient to divide
the mass of metal into small parts, which soon took the
form of rough coins. But the principle of payment by
weight was retained through many centuries, and is per-
petuated, though in name only, in the word " pound."
Records of attempts to organize the coinage of England
are found as far back as the Anglo-Saxon period, and it is
known that on the dissolution of the Heptarchy the mints
were regulated by laws framed in the witenagemot. The
first monarch who appears to have dealt successfully with
the organization of the coinage was Athelstan, who framed
laws for the regulation of the mints, and appointed officers
whose titles and duties are then first recorded. The only
officers connected with the coinage of whom mention is
found before this time are the " moneyers," who appear to
have been alone responsible for the manufacture of the coin ;
but it is probable that even then there existed some ofiicer
who had authority over them. In early Saxon and Norman
times the number of moneyers V'as considerable, mints
being established in almost every important town, as might
be expected at a period when communication between
distant places was extremely difficult. They appear to have
been the officers who actually performed the work of
making the coin, the mint master in later times contracting
with them, at a high rate, for the work. They were respon-
sible for the piu'ity and perfection of the coins produced,
as appears from the fact that it was they who were
punished (as traitors) in the case of any deficiency in weight
or fineness. They had prescrijitive rights in the coinage,
and in modem times (even so late as 1850) claimed to have
corporate privileges ; but it is clear, on the authority
of Ending, that they never were a " corporation " separate
from other officers of the mint.' The number of mints
was greatly reduced after the Norman Conquest, but
continued to be considerable until the reign of Kichard L,
when the work of coining for the whole kingdom was con-
centrated in the mint in the Tower of London. Only one
provincial mint (Winchester) remained till a later date.
An important reorganization of the coinage took place
in 1325 under Edward II., the regulations then framed for
the manufactitfe and issue of the coins forming the basis
of those still in force. The principal officers under these
regulations were — master, warden, comptroller, king's assay
master, king's clerks, and cuneator. The ofiice of cuneator
was one of gi-oat importance at a time when there existed
a multipUcity of mints, since he had the sole charge of all
the dies used not only at the mint in the Tower of London
but also in the provinces. He chose the engravers and
presented them to the barons of the exchequer in order
that they might take the oath of fidelity ; he superintended
their work, and was generally answerable for the perfection
of the dies before they were issued for use in the various
mints of the country. The office, which was hereditar)',
ceased to exist when the provincial mints were suppressed.
In its place was instituted the office of clerk of the iron,-,
* Among tho Kpeciftl privilege which thoy undoubtedly enjoyed w;i
oxoniption from local taxation, as nppojira in a "writ of Henry 111.,
which commands the mayor of London not to disturb them ' ' h\
exacting tallages contrary to their privileges." Sometimes also house:
were allowed to them rent frcfi.
MINT
481
-whose f anctiona were more limited, and %/ere not hereditary.
This ofSce was only recently abolished.
In the Middle Ages an important duty devolving on the
officers o£ the mint was the collection of the seigniorage
which was levied on the coining of money, not only for the
purpose of covering the ejcpenses of minting, but also as a
source of revenue to the crown which the sovereign claiined
by virtue of his prerogative. In former times the collection
of the seigniorage was entrusted to the warden, who also
superintended the manufacture of the coins, so far as to
ensure the proper relations between the moneyers on the one
hand and the state on the other. He does not appear,
however, to have had any responsibility with regard to the
fineness and weight of the coins.
The king's sissay master was specially charged with all
matters relating to the accuracy of the standard. The officer
next in rank to ti'm was the comptroller, who presented
annually to the barons of the' exchequer a report of all the
gold and silver money struck in the kingdom during the
year. These reports, which were always written upon
parchment, constitute the chief mint records. The king's
clerk exercised a general superintendence and kept an
account of all the mint transactions. As the work of the
mint became more extensive and more complicated, other
officers were added such as the surveyor of the meltings,
sorveyer of the money presses, and many others.
The present arrangements with regard to the officers of
the mint were made in 1870, when several important changes
took place in the mint establishment. Up to that time
there had been two controlling officers, — the master, who
in some instances was selected on account of distinguished
scientific attainments (as in the cases of Sir John Herschel
and Professor Graham), and the deputy master and comp-
troller. A careful inqiiiry, however, having led to the
conclusion that the control of the mint might with advantage
be concentrated in the hands of a single officer of experience
in the conduct of public business, it was decided, on the
death of Professor Graham, to entrust the actual adniinistra-
tiou of the department to the deputy master, — the office
and title of master of the mint being held by the
chancellor of the exchequer for the time being, without
salary. At the same time the services of a scientific officer
were secured, by the appointment of a chemist of the mint.
The coining and die department and the melting depart-
ment were united under the name of the operative depart-
ment, and placed under a single superintendent. The
first deputy master appointed under the new regulations
was the Hon.' C. W. Fremantle, C.B., to whom the public are
indebted for a series of Annual HeporU which have given a
new and increased interest to the subject of the coinage, and
may be said to constitute in themselves a mint literature.
"The actual operations of coining in early times were few
in number and simple in character. The metals forming
the alloy were melted together in the proportion necessary
to bring them to the required standard, and the alloy thus
obtained was cast into bars, which were reduced by
hammering to the requisite thickness. They were then
cut with shears into piepes more or less regular in size and
form, roughly annealed, and finally impressed with the
prescribed device by a blow with a hammer.
The last-named appears to have been the only part of
the process which was performed with any great amount of
care. The blank piece was placed by the hand upon a die
fixed into a block of wood having a large heavy base to
resist the oscillation caused by the blow ; the die on which
was engraved the device for the reverse of the coin was
then placed upon the upper side of the blank and held by
means of a holder, round which -was placed a roll of lead to
protect the hand of the operator while heavy blows were
strack with a hammer by an assistant workman. «.One of the
earliest improvements in coining was the introduction of a
tool in shape resembling a pair of tongs, the two dies being
placed one at the extremity of each leg. This avoided the
necessity of readjusting the dies between successive strokes
of the hammer, and ensured greater accuracy in the impres-
sion. It was long before the system of coining by hand was
superseded by the coining press, or mill, which, even after its
first introduction, was only very slowly adopted. Several
attempts were made to introduce machinery for coining
before it was brought into active use, the objection to it
being its great expense. The mill and screw were finally
introduced into the mint under Charles II., when many
improvements were also made in the preliminary operations.
Steam-power -was first applied in 1810, when the vacuum
screw-press -was introduced. In 1839 Uhlhom invented the
lever-press, which still remains in use.
The subject of the design on coins, besides being inter-
esting both from an artistic and an historical point of view,
becomes very important when it is remembered that it is
the impression of the coin with the authorized device
which makes it legally current. The artistic merits of the
design of the early Greek coins are well known, and prove
that the dies from which the coins were struck must have
been engraved with much skUl and care. The form of the
coins before being stamped was at first merely that of
natural rounded nuggets of gold, or of the silver-gold alloy
known as electrmn. Such coined nuggets of gold ai-e still
to be found among the hill tribes of India. Simple
nuggets were aftem-ards replaced by roughly-fashioned
masses like half bullets, a form which rendered it easy to
impart high relief to the obverse and comparatively low
relief to the reverse of the coins. The early British coins *
had for their prototype the gold "stater" of Philip of
Macedon, but the design of this beautifully finished coin
was so roughly imitated by a succession of British copyists
that ultimately the •wreath round the head of the monarch
alone survived, and that in a scarcely recognizable form.
It is not only in the early British coins that the influence
of classical art may be seen, for it is very evident in some
of the present day, the most notable instances being the
reverse of the bronze coinage, and the beautiful design of
St George and the dragon by Pistrucci, which is still used
as an alternative design for the sovereign. It has been
ascertained that the impressions on the reverse of very
early Greek coins were produced by the rough surface
of the anvil or the nail head on which they were placed,
while the obverse was struck with the die. A little later
the device on the reverse of the coins was obtained by
placing the blank piece on small points of metal arranged
in geometrical forms which caused corresponding indenta-
tions on the coins when struck with the hammer. The
beauty and accuracy of design on coins gradually increased
as art and manual skill developed, and probably culminated
at the period of the Renaissance.
Although it has been the custom since the time of the
Saxons to stamp coins -with the head of the reigning
monarch, it does not appear that any attempt at actual por-
traiture was made in England until the reign of Henry Vll.,
who, " about the eighteenth or nineteenth year of his reign,
did make a great alteration in the form of his coin, upon
which his head was now represented in profile, and with
a good resemblance of his other pictures."- Since then
much care seems to have been taken to stamp the coins
with a true likeness of the monarch. In most cases the
heads bear a striking resemblance to the portraits dra^wn
by the great artists of the respective periods, and were,
indeed, generally designed by artists of eminence. Some
of the Milan coinage of Louis XIL is said to have been
' See Evans, Coins of the Ancient Britons.
" See Martin Folkcs. JoSJm of English Silver and QoUC Coiat
iYL — 6 I
482
MINT
designed by Leonardo da Vinci, and similar work is attri-
buted to Benvenuto Cellini.
In very early times the silver coins were equal in weight
and in tale, each penny weighing 24 grains or 1 penny-
weight. Tlie amount now denominated a pound was a
pound weight of standard or sterling silver. This principle
was in fact, however, not strictly adhered to, the coins
frequently falling below the standard of weight. This
deviation may possibly have arisen from the imperfection
of the methods of manufacture, but Ending {Annals of the
Coinage) considers it to have occurred from design, as the
deficiency in weight was sometimes made a source of profit.
The deviation from the standard weight permitted by law,
now called the " remedy," and anciently called the " shere,"
was taken advantage of to a large extent, so that the coins
suffered considerable diminution, particularly when, as
frequently happened, they were also " clipped " as soon as
they were issued. 'WTien these coins were called in they
were taken by weight and not by tale, so that the posses-
.sors suffered considerable loss. In later times the great
improvements in the method of manufacture made it easy
to attain far greater accuracy both of weight and fineness ;
consequently the remedy permitted by law has been con-
siderably reduced, and the possibility of making a large
amount of profit by this means proportionally diminished.'
The seigniorage levied on the coining of money was not
a fixed rate, but varied considerably at different times, and
accrued from a deduction made from the bullion coined.
It was abolished by an Act of Charles IL, which provided
that whoever brought sterling silver or standard gold to
the mint should receive in exchange an equal weight of
current coin, the expenses of coining being defrayed by
means of duties levied upon certain commodities of common
use. The seigniorage on silver was revived in the reign
of Georgo III., when that part of the Act of Charles II.
which related to the coining of silver without charge was
repealed, and another Act was passed, requiring every
pound of silver to be coined into sixty-six shillings instead
of sixty-two, — the four shillings realized on each pound of
silver by this depreciation of its value being handed over
to the master of the mint to defray the expenses of assay-
ing, loss, and manufacture. An Act of William IV.
required the seigniorage on the silver coinage to be paid
to the credit of the Consolidated Fund, and the charges of
the mint to be brought annually before parliament. Against
the profit derived by the state from this source must be
placed the expense of maintaining the silver coinage in a
condition fit for circulation by frequently withdrawing,
recoining, and reissuing the silver coins. A vote of
£15,000 is annually taken in the mint estimates for the
loss on the rccoinago of silver.
In former times the work of the mint was performed by
contract, the mint master undertaking the manufacture of
the coinage at a stated price, and paying the moneyers
and other officers and workmen under him at a fixed tariff.
The agreement made between the crown and the mint
master, called the "master's indenture," was sometimes
purposely kept secret. This system appears to have pre-
vailed from the reign of Edward I., when an agreement
was entered into between the king and the first master of
the mint (appointed about 1279). Under this agreement
• Two noUiblo instances are rccorilod of tlio use tliat has liccn made
at various times of tiio shero, or remedy, as h means of profit, one
being in the reign of Queen Elizabeth, when Lonison, then master of
the mint, finding tho allowance made him under his contract was in-
nufRcient to cover tho expenses of coining, availed himself of tho
remedy on tho silver coinage, amounting to 6jd. in tho pound troy.
The olhor ocoiirrtd at the time of the gieat lecoinngo of silver in tho
reign of WiUirvm III., when tho profit of tho shere amountod to 3d.
per pound wgight, or rather mora than 8s. in ovary hundred pounds
of xnonef •
an allowance was secured to the master to cover all the ex-
penses of coinage. Although the master of the mint ceased
to be a contractor, the arrangement with the managers con-
tinued in force up to 1851.
The work of coinage was transferred in 1810 from the
Tower of London, where it had been carried on for many
centuries, to the present Mint on Tower Hill, not far from
the Bank of England. The head of the department, as has
already been stated, is the chancellor of the exchequer for
tho time being, who is ex pfficio master of the mint, — the
practical direction of the work being placed in the hands
of a permanent officer, the depu ty master, who is responsible
for its due performance. From the English mint is supplied
the coinage for the whole of the British empire, including
the colonies, with the exception of Australia ; the latter
and the East Indies are supplied from branch mints estab-
lished at Sydney and Melbourne, and the mints of Calcutta
and Bombay. In addition to the gold, silver, and bronze
coins current in the United Kingdom, the English mint
strikes gold coins of the value of two dollars for New-
foundland ; silver coins of the value of fifty, twenty-five,
twenty, ten, and five cents respectively for Newfoundland
and Canada ; bronze pence and halfpence of special design
for Jersey, and nickel pence, halfpence, and farthings for
tho West Indies. The number of coins of each separate
denomination issued varies considerably in different years,
the demand for special denominations of coin naturally
determining the supply.
The following table (from official sources) sljows the value of the
gold and silver coins issued during the ten years 1871-81. The
total value of the bronze coin issued in the same peiiod is £112,890.
Dale.
Gold Coinage.'
Silver Ci'lnnge. |
Sovereigns.
Half-Sovereigns.
Total Value.
Half-crowns.
Florins.
£
£
JE
£
£
1872
13,043.885
1,617,550
15.201,441
092,010
1873
2,382,835
1,001.733
3,384,608
5!i0,574
1874
519,029
941,930
1,461,505
273.240
180,774
1875
.
243,204
243,204
138.990
114,246
1876
3,294,705
1,401,943
4,096.648
79,200
00.78S
1877
981,403
981,408
1878
1,106.289
1,158,730
2,205,069
183,150
178,590
1879
17,625
17,525
36,050
112,002
13.-..432
18S0 ,
8,640.853
504,199
4,150,062
108,102
232.254
1881 '
256,800
24,610,721
7,868,408
32,479,129
1.29l,3-.0 , 2,610.184 1
Date.
Silver Coinage
J
Shillings.
Six-
pences.
Four-
pcnrca.
Thrcc-
pcncos.
TVo-
penccs.
Pence.
Totals.
£
£
£ «.
£ s.
£ 1.
£
£
1872
443.322
94,446
69 6
13,916 2
39 12
33
1.243.836
1873
324,324
109,890
69 0
50,744 2
.19 12
275.022
10.-.,732
69 6
66.694 2
1876
217.800
81,378
69 0
41,433 3
39 12
1876
38.412
20,988
69 0
22,826 2
39 12
1877
103,3.50
101,772
69 C
31,142 2
166,222
05,638
69 C
30,360 2
180.676
83,160
69 6
37,082 2
39 12
649.054
96,426
09 0
22.430 2
1881
262,648
166.816
09 6
40,640 2
2,303,730
916,146
693 0
346,209 0
390 0
330
7,376,104
The British sovereign or twenty-shilling pirco wag fii-st issued
by proclamation dated 1st July 1817, supcrsodiiig the guinea or
twenty-one-shiUing piece. Crown pieces of the nominal value of
five shillings were first struck in the reign of Henry VIII., si.\-
iiences and threepenny-pieces are first mentioned in the reign ol
Edward YI., while the groat or fourpenny-pitcc was coined as early
as the reign of Edward I. ; tho florin or two-shilling-pieco was
introduced" in 1849. Copper money was fiist coined by Charles I.
ill 1606, but docs not appear to have been issued until 1672. Copper
was replaced by bronze in 1860.
Tho weight and finene.ss of the various denominations of coin
struck at tJio Royal Mint is shown in tlie first sclicilule of the Coin-
ago Act (33 Vict, c. 10), 1870 :—
5 In these gold returns fractions of pounds sterling are omiited.
' The numbers and weights of Uie fourpences, twopenccs, and pence,
being Maundy coins, are the same for each of the years : — 4618 four»
peaces, 475- twopences, and 7920 pence.
MINT
483
Denomination of Co
Stanibinl Weight.
Imperial
Wclglit.
Grjlns.
Least Current Weight.
ImperiM
Weifiht.
Grains.
Slclrlc
Weight.
Grammes.
Remedy Allowance.
Weight per Piece.
Gold—
Five pound ,
Two pound.
Soveriign
Half-sovereign
SUver —
Half-crown..
shuiing'."!'.!'.!!!!!!'.!!!
Sixpence ,
Groat or fonrpence...
Threepence
Twopence
«l(;-37239
2M M895
lS-3-27447
6103723
436'383SD
31618181
VUhVAb
87-2T27J
43'63<J36
2909O9O
2181818
7-27273
14S'83333
87-50000
43'71>0OO
3»040!8
1S07C11
7-0S800
8-99402
28-27590
1413795
11-31030
505.^18
282759
1-8850S
14I379
0-94253
0-47128
9-449S4
swaoo
2-83495
612-50000
24300000
122-50000
61-12500
39-68933
15-87574
7-93787
{) fine gold, A
alloy; or milled
fiimal fineness
91661;.
millesimal
fineness
and i.
1-00000
040000
0"J»000
0-lOUOO
1-8181S
0-90909
0-72727
0-36363
018131
0-12121
009090
0-06060
0 03080
2916e6
1-75000
0-87500
0-06479
0-02.'.92
0-01296
0-00643
0-11781
0 05890
004712
0-02356
0-01178
00078S
000589
0-00392
0-00196
0-1,1899
011339
005669
The weight and fineness of the eoins specified in this schedule
ire according to what is provided by the Act 56 Geo. III. c. 68,
that the gold coin of the United Kingdom of Great Britain and
Ireland should hold such weight and fineness as were prescribed in
the then existing mint indenture, that is to say, that there should
be nine hundred and thirty-four sovereigns and one ten-shilling
piece contained in 20 lb weight troy of standard gold, of the fine-
ness, at the trial of the same, of 22 carats fine gold and 2 carats of
alloy in the pound weight troy, and further, as regards silver coin,
that tliere sliould be sixty-sLx shillings in every pound troy of
standard silver of the fineness of 11 ounces 2 pennyweights of fine
silver and 18 jicmiy weights of alloy in evei-y pound weight troy.
The jTcscnt standard of fineness for gold, 22 parts line or pure
gold aud 2 parts of alloyed metal, was finally adopted in the reign
of Charles II., and has remained unchanged up to the present
time. Before the passing of the Act determining this standard
considerable changes had been made from time to time, the highest
degree of fineness having been reached in the reign of Henry 111.,
when the first gold coins were struck of the standard of 24 carats
pur« gold. The standard of fineness for gold at some different
periods may be seen from the following table, which shows the
composition of some of the ancient gold trial plates, of which
portions are preserved in the Mint : —
Date.
Standard prueribed
by Law.
Standard
foimd by
.\8say
Remedy or
In Carats
and Gruins.
Decimal
Ennlvalent.
In Carats and In
Thousandths.
1349
\ carat, or 13 9
1477
23 31
994-8
Gold 993-5
.. .. '•»
1527
22 0
91C-6
,. 913-5
.. » C-9
1643(1)
23 0
958-4
„ O-VI^
., ,. 69
1553
23 31
994-8
„ 990-3
.. ,. 6-9
1560
22 0
916-6
„ 913-7
» 1. «9
1560
23 i\
994-8
, 994-3
.. ,. «•»
1593
22 0
916-6
„ 915-9
„ „ 6-9
IC05
23 31
994-8
„ 990-3
.. .. «•»
1049
22 0
9ii;'6
, 9130
.. ,. 69
1660
23 3}
994-8
„ 990-9
„ „ 6 9
1660
916-6
., 012-9
.. .. «■"
ie«3
22 0
916-6
„ 914-6
>. .■ "9
1707
22 0
916-6
„ 9171
M ,• 69
1728
22 0
9160
, 916-1
.. .. 6-9
IfiO
22 0
916-6
„ 915-3
U .. .. 26
1873
22 0
916-6
., 916-61
20
1873
Eupplementaiy plate.
Pure ROlJ.
...
The earliest trial plate of which there is any record was made in
the seventeenth year of Edward IV. Before that time it would seem
that the coins were comfiared with otliers known to be of standard
fineness, since among the Cotton MSS. is preserved the account of
the trial of the pyx of gold nobles in 1349, when the coins were
compared with an ounce of florins of Florence kept in the Treasury
as standards. The first gold coins were 24 carats fine or pure gold.
Edward III. caused coins to be struck of 23 carats 3^ grains fine
in 1346, but no trial plate of this standard was made until 1477.
Henry VIII. lowered the standard to 22 carats, but caused coins
to be struck both of that and the former standards. The greatest
debasement of the standard ever reached in England was in
1546, when it sunk as low as 20 carats. It reached a low
r point in the early part of Edivard VI. 's reign, but was raised
towards the end of it to 22 carats ; and it was still further raised
to 23 carats Z\ grains by Elizabeth, who, however, caused gold
coins of 22 carats also to be struck. Charles II. on his accession
rejected the trial plates of the standard of 22 carats which had
been made under the Commonwealth, and caused others to be
made of the standard of 23 carats 3^ grains. No coins, however,
appear to have been struck of this standard. The same monarch
afterwards fixed the standard at 22 carats ; and no variation in ths
legal standard has occurred since that time. The last new trial
plates, made in 1873, were alloyed with copper only, in order that
they might correspond with the composition of the British gold
coins, former plates having been alloyed with silver and copper.
At the same time supplementary jdates of pure gold and silver
were prepared in order that the greatest possible accuracy might
be secured.
The present standard of fineness of silver for coinage was fixed
at a very early period, but has been subject to considerable varia-
tion since the reign of Edward I., the first English monarch who
debased the silver coinage. In the reign of Henry VIII. it was
once reduced as low as 4 ounces of silver to 8 of alloying metal,
and Edward VI. reduced it oven lower. It was restored by
Elizabeth to the original standard.
The following table shows the composition of some of the ancient
silver trial plates of which portions have been iireserved in the
Mint :—
Dato.
Standard prescribed
by Law.
SUndaM
found by
Assay.
Remedy or
Permitted Variation
In Dwts. and in
Thousandths.
In 023.
and dwts.
Decimal
Etjnivaient.
Ko date.
Silier 767-4
1477
11 2
925-0
„ 923 5
3 dwts.
1527 (?)
„ 8855
1542
9 6
775-0
„ 763-6
3 dwts. (?), or 12-i
1553
11 2
9250
„ 827-0
Sdwta^ or e-4
1560
11 2
925-0
„ 930-2
2 >. » 8-4
160O
8 0
250-0
„ 252-0
3 „ „ 12-5
1601
11 3
925-0
„ 925-1
2 IP .. 8-4
1604
11 2
9250
„ 922-7
2 dwia.
1049
11 2
9250
„ 923T
2 ..
1660
11 2
925 0
„ 924-2
3 dwts., or 8 4
16SS
11 2
925-0
,. 922-0
2 i, .. 8-4
1707
11 2
9250
„ 0220
2 „ „ 84
1728
11 2
9250
. 9-JS-9
2dn1s.
1829
11 2
925-0
„ 925-0
1 dwt.. or 4-2
1873
11 2
9250
„ 92496
4-0
1873
Supiilementary pinte.
Pure silver.
The alloy used for the bronze coinage is composed of 95 per cent,
of copper, 4 of tin, and 1 of zinc. The bronze coinage superseded
the old copper coinage in 1860, the latte;- having been in use since
the reign of Charles II. The vicissitudes of the copper cQinage
were even greater than those of the superior coinages, coins for
Ireland having been issued at one time of pewter and of other
alloys in which scarcely any copper was contained.
The annual testing of the standard of gold and silver
coins, called the trial of the pyx, from the " pyx " or chest in
which the coins to be examined are kept, is a ceremony of
very ancient institution. It arose from the circumstance
that the mint master was originally a contractor, under the
crown, for the manufacture of the coinage, and it was
therefore necessary that periodical examinations of the
coins should be held in order to ascertain that the terms of
his contract had been complied mth. At the present day,
when the mint master is no longer a contractor, but an
officer of the crown, the trial of the pyx has a somewhat
different object; but it would appear from the description
of these periodical examinations in some of the earliest mint,
records that but little change has taken place in the manner
of conducting them. The finished coins are delivered
to the mint master in weights called "journey weights,"
484
MINT
suj^osed to be the weight of coin vrhich could be manu-
factured in a day when the operations of coining were
performed by the hand. The journey weight of gold is
15 lb troy, coined into 701 sovereigns or 1-102 half-
sovereigns. The journey weight of silver is 60 lb
troy. From each journey weight a coin is taken and
deposited in the " pyx " or chest for the annual trial. This
is made by the freemen of the goldsmiths' company under
the direction of the crown in the presence of the queen's
remembrancer, who administers the oath to the jury and
presides over the proceedings. The coins selected for trial
are compared with pieces cut from trial plates of standard
fineness, which are in the keeping of the warden of the
standards, these pieces being assayed against the coins
under examination. K the coins are found to be of the
standard fineness and weight, within certain limits, a verdict
to that effect is drawn up by the jurors and presented to
the Treasury.
In consequence of the impossibility of ensuring an abso-
lutely exact admixture of metals in coining, it has been
Boand necessary at all times to allow to the mint master
a certain margin, or "remedy," within which coins may
savy in weight and fineness from the fixed standard and
still be considered of the current standard. The remedy
of fineness for English gold coin is now fixed at 2 parts
per 1000. The great importance of maintaining the
standard of fineness for gold will be evident when it is
stated that the variation of y'^j of a millifeme (or thou.sandth
part) above or below the standard causes a gain or loss
of ilOO in every miUion sterling. Gold coins would
be within the remedy of fineness permitted by law if
the amount of precious metal contained in them varied
from 914-6 to 918-6 parts in 1000; and, although this
remedy caimot be considered to be more than would
meet occasional and unavoidable deviation from the exact
standard, still, in the case of gold, but a very small part of
the remedy of fineness is actually used, the coins seldom
falling below 916-3 parts of gold in 1000, or rising above
917-0, while the mean composition of many millions of
coins issued from the mint is often of the precise legal
standard, 916-65. The remedy of fineness for silver coin,
which appears to have been always greater than that for
gold coin, is 4 parts per 1000. The remedy of weight
for 2;old is 1--6 per 1000 parts, that for silver 4-17, and
that for bronze 20. Extreme care is taken to prevent the
issue from the mint of any coins that exceed these permitted
variations in weight and standard, each coin being weighed
separately, and all those found to be above or belo-w the
standard being returned to the melting-house.
Since the real value of the gold coinage is the same as
its nominal value, it is of the first importance that gold
coins which are below the standard weight should not be
allowed to circulate, otherwise holders of large quantities
of gold coin are liable to considerable loss. After a certain
amount of wear a gold coin in passing from hand to hand
loses weight and becomes legally uncurrent. By the Coinage
Act it is made compulsory for every person to " cut, break,
or deface " any coin tendered to him in payment which is
below the current weight, the person tendering it bearing
the loss ; but, as no penalty is imposed for disregard of this
obligation, the law is practically without effect. The
withdrawal of light coin from circulation was formerly
accomplished solely by the Bank of England, the mint
regulations making provision for the receipt cf gold tendered
for coinage only in the form of bars. The bank undertook
to purchase the light gold from the public at the rate of
£o, 173. 6Jd. an ounce, a price which, as compared with
the mint value of £3, 17s. lOtd., entailed a loss of no less
than 4d. an ounce on the seller. This loss was occasioned
chiefly by the circumstauce that the baak, being obliged
before sending the light gold to the mint for recoinage to
melt, assay, and cast it into bars, found it necessary to
deduct the sum of 2id. an ounce from the rate of £3, 17s.
9d. an ounce at which it was allowed by statute to purchase
gold for coinage, in order to cover the expense of these
operations and the loss incident to them. The heaN-y lois
in price, added to that from deficient weight, occasioned
constant disregard of the law requiring all light coin' to be
cut or defaced, and consequently a large amount of light
gold continued to be circulated. After the passing of the
Coinage Act in 1870, accordingly, fresh regulations were
made, by which the mint authorities undertook to receive
light gold coin for recoinage, returning to the importer the
full mint value of £3, 17s. lOJ-d. an ounce, thus reducing the
loss to that arising from deficiency of weight only. As the
Bank of England was enabled by these regulations to raise
its price for light gold to the rate of ,£3, t7s. 9d., the same
rate at which it is bound to purchase ingots of standard
gold, greater inducements were offered to the public to seud
in light gold for recoinage, and its withdrawal from
circulation was in consequence greatly facilitated. It is
evident, however, that, as the deficiency in weight must
entail some loss on the holders of light gold coin, they will
be disposed to keep it in circulation as long as possible ;
consequently only a small proportion of the light gold
received by bankers finds its way to the Bank of England
and thence to the mint for recoinage. The result of some
careful experiments made by the late Jlr Stanley Jevons,
and published by him in the Journal of the Statistical Society
(vol yxxi. p. 426), showed that a sovereign becomes so
light as to be legally uncurrent at the end of eighteen years.
The last state measure taken for the vvithdi-awal of light
gold coin from circulation was the issue of a royal jiro-
clamation in 1842 calling attention to the laws and
regulations relating to light gold coin, and instructing
those persons whose duty it was to enforce them to see
that they were carried out. From the beginning of July
1842 to the end of March 1S15 £14,000,000 in light
gold coin was withdrawn from circulation and recoined.
This amount was estimated to represent 95 per cent, of the
whole of the light gold then in circulation. In order to
facilitate this withdrawal the Treasm-y had in .June 1842
entered into arrangements with the Bank of England by
which the bank was enabled to purchase light gold on
behalf of the Government, at the full mint value of £3, 17s.
lOid. an ounce. Light coin, however, continued to be
sent into the bank for some time after it had reverted to
its original rate of payment for light gold, i.e., £3, 1 7s. 6^d.
an ounce. The expense to the state of this withdrawal,
including the expenses of recoinage, was £67,816. As no
important withdrawal of worn gold coin has occurred since
that time, it is evident that a large amount of light gold
must bo at the present time in circulation, and that the
loss in weight must be considerably greater than that of
the coins withdrawn in 1842, the oldest of which were not
more than twenty-five years old, the first issue having taken
place in 1817. It has been proved by experiment that the
average loss of weight in worn sovereigns and half-sovereigns
now in circulation is about 3d. in each sovereign, and that
the deficiency in fineness of a large proportion of the coin
amounts to about £400 per million. This deficiency arises
from the trial plate of 1829, which determined the standard
of a portion of the coins still in circulation, being itself
below the legal standard. Taking the gold circulation at
£100,000,000, of which about 50 per cent, is light, it is
estimated that the amount to bo recoined cannot be less
than £50,000,000, on which the loss from deficiency of
gold, both in weight and fineness, must be reckoned at about
£660,000, independent of the expen.ses of recoinage.
In the case of the silver coioage, the loss consequent on the
MINT
^5
Uithdi-awal and recoinage of silver money is now covered
•by the seigniorage arising from the difference between the
real and the nominal value of the coins. Before. the adop-
tion of gold as the sole standard of value, the conditions
attending the withdrawal and recoinage of silver were much
the same as those for gold. In the period between the reign
of Charles n. and the accession of William III. the
condition of the silver coinage became so unsatisfactory as
to demand the attention of parliament. A recommendation
made at the suggestion of Sir Isaac Newton for a recoinage
of silver was at first strenuously opposed, but was finally
adopted. In the. course of the discussion the question of
raising the standard of weight and fineness arose, and this
important change would probably have been made but for
the representations of Locke, jvho warmly took up the
question and convinced the Government of the desirability
of preserving the established standard. In the great
recoinage of silver, the loss arising from clipped and defaced
coin was borne by the public, the money being raised by
means of a special tax on glass windows. The silver
reissued at this time amounted to £7,000,000, and the
tax raised to cover loss and the expenses of coinage to
£1,200,000. The work of this recoinage was so great that
the resources of the mint in London were found to be
unequal to the pressure put upon them, and therefore
mints were either revived or established for the first tin.e
in a few of the large provincial towns. In addition to
this ten furnaces were erected behind the Treasury at
Whitehall to melt down the old pieces. By these means
the renovation of the silver coinage was completed within
the year. The new silver coins then issued were the first
which had milled edges, the milling having been introduced
in order to prevent clipping.
The mode in which the silver currency is distributed throughout
the kingdom is explained by the late Mr George Forbes, cashier of
the Bank of England, as foUows : —
Every banker in the kingdom has a banker who is his agent in
London. Every London banker has an account with the Bank of
England. In the Bank of England there is a department devoted
to the issue and receipt of silver coin. If in a district there is a
deficiency of silver currency, the bankers of the district arc tho first
to find it out Tliey at once writo to their London agents, who
draw on their account with the Bank of England, and obtain what
■silver is required, wliicli they send to tlie country banker. On tho
other hand, if there is a surplus of silver in a district it accumulates
in tire coffers of the local bankers, who send it up to their London
agents, and they send it into the Bank of England. If there is a
^enei'al demand for silver cuiTency, the stock which tho Bank of
Eirgland endeavours to keep on hand becomes unduly diminished,
and immediate notice of tlic fact is conveyed to the mint authorities,
who proceed with all convenient speed to coin a supply of florins,
Bhillings, sixpences, or of all of these coins, as the nature of the
(Rmand may require.
Gold bullion for coinage is supplied to the mint almost
entirely by the Bank of England, the bank being bound
by law to purchase at the rate of £3, .17s. 9d. an ounce
any gold bullion of the legal standard which the public
may bring for sale. Private individuals are permitted to
bring bullion to the mint, and to receive back the full
amount (at £3, 17s. lOid. an ounce) converted into coin,
free of any charge for loss or manufacture ; but, as they are
subject to considerable delay, all " importations " of bullion
being converted into coin in the order in which they are
brought to the mint, the public practically prefer to sell
their bullion to the bank, and receive its value without
delay. In order to be accepted by the bank, the bullion
must be cast into ingots and assayed, a guarantee being
^vcn by certain recognized assayers that the gold is of a
certain standard fineness. This is known as the " trade
assay." When the bank requires gold to be struck, due
notice is sent to the deputy master, and on a fixed day
the bullion is conveyed to the mint and delivered into hb
custody. It arriv<)si in the form of ingots, each weighing
about 200 ounces, the aggregate value of each importa-
tion being about £144,000. When the ingots arrivq at
the mint a small sample is taken from each and assayed,^
tho result being sent to the authorities of the bank in
order that it may be compared with that of the trade
assay. If the bank authorities find that the two assays
agree, within certain limits, as to weight and fineness, the
ingots are immediately sent to the operative department of
the mint to be converted into coin. The mint assay affords
the basis for calculating the amount of copper, the alloying
metal, that must be melted with the gold in order to produce
the standard prescribed by law. The case of silver is
somewhat different, the bullion being purchased by the
department at its market value, which varies from year to
year. During the teruyears ending 1881 the average price
of silver bullion sank gradually from 60j^d. to Sly^.
The silver bullion arrives at the mint in the form of ingots,
each of which weighs about 1000 ounces, the value of each
set of ingots varying considerably. The ingots, both of
gold and silver, are weighed on a balance capable of turn-
ing with 1 grain when loaded with 1200 ounces.
The operations of coining have undergone some sUght
changes with the introduction of new machinery and the
increased extent of the Koyal Mint, since the reconstruc-
tion of the operative department in 1881.^ The. plan
(fig. 1) shows the present arrangement of the operative
department.
The operations employed in the manufacture of gold ajid
silver coin are as follows (incidental operations teing
printed in smaller type) : —
I. Assaying the bullion.
II. Melting the metal.
(o) Addition of the amount of copper necessary to f-jrni
the prescribed alloy ; (b) poirring the metal into mo'.ilds
so -aa to form bars ; (c) dressing these bars to remove
rough edges and hollow ends ; (rf) recovery of procioua
metals from crucibles and "sweep."
III. Assaying portions of metal cut from certain bars,
to ascertain whether sufficient accuracy has been attained
in the standard fineness.
IV. Kolling the bars into strips or " fillets."
Annealing the fillets (in some cases).
v. Adjusting the fillets by a final rolling, and in aouie
cases by the use of the drawbench.
Testing the fillets to ascertain whether they are of fiwTi^
cicut accuj;acy as regards thickness.
VX Cutting out disks or blanks from the fillets.
Adjusting the blanks in weight (in some mints).
Vn. Edge-rolling the blanks to produce a raised rim.
Annealing the blanks and (in some cases) "blancfeiirg -
or " pickling" them in dilute acid.
Vni. Coining, or stamping the device on the blank^ by,
means of engraved steel dies.
Milling the edges of the blanks or (in some cases) im^
pressing a device, inscription, or ornament upon tbera.
IX. Weighing each coin, usually by the aid of automatic
machinery.
X. Assaying and weighing pieces taken fronrsthe
finished coin before it is issued to the public.
The foregoing list will make it clear that the operatic«s
of minting consist, not .simply in the mechanical production
of accurately adjusted disks of metal the purity alone of
' The assays are conducted in the manner already described in the
articles AssATDfo and Gold;
' In order to provide a stock of silver coin during the temporary
suspension of the work of the mint, a large coinage of silver was ifsued,
and 50 tons of brorrze coins were manufactured by contract ia the
autumn of 1881. The governor of the Bank of England had ptevkrusiy;
reported that the stock of gold coin held by the bank was abnonnalljj
large, and that no inconvenience would arise "if the mintwci«toeeasa
coining sovereigns and haif-sovereigns for a period of sirmonths or-»
year or even more,"
486
MINT
iwhich has to be guaranteed, but in the formation of an
alloy composed of j)rcciou3 and base metals in definite pro-
portions. The accuracy of the "standard fineness" of the
alloy after melting must be absolutely ascertained; the
alloy must be protected duiing manufacture against a
change of standard, and finally its correctness must be
verified after it has been converted into coin.
The precious metals are weighed on entering the mint,
OB well as during various stages in the manufacture of
coin. The finished coins are also weighed in bulk before
they are issued to the public.
The operations incidental to the coinage of bronze and
silver differ from those described in relation to gold in some
unimportant details only; and the weight and composition
of the bronze coins are not so carefully guarded as ig the
case with gold and silver.
Subjoined are the details of the operations involved in'
the conversion of bullion into coin at the British mint.
After beingassa3'ed and weighed in the manner already described Mettiii^
the bullion is taken to the nieUing-housc, where the details of treat- the
nicnt for silver and gold respectively dilfer somewliat, (The sub- metaL
sequent operations are nearly identical for both metals. ) The
silver melting-house (see fig. 1) contains eight furnaces, of the
kind shown at A fig. 2, the ^Kirt of the furnace containing the
crucibles being below tlie lids B, B. Crucibles of cast iron were
formerly employed, but these were replaced in 1853 by wrought
iron pots, which have since 1870 been m turn abandoned in favour
of crucibles made of a mixture of clay and graphite, cacli crucible
being capable of containing about 3000 oz. Such crucibles are
very generally adoj)ted throughout the Indian and Continental
mints, but the form and dimensions given to them vary. The
fuel employed in England is coke, about 75 lb of which arc re-
quired to melt 3000 oz. of standard silver. Sufficient draught is
afforded by the flue C and by a chimney about 35 feet high wliicli
communicates with it. The silver and copper are melted togct!"r;
MAIN BUILDINQ v
(OFFICES iP) \ /
MINT
OFFICE
iMi
Fto. 1. — Royal Jlint, Tower Hill, London. Plan showing the Operative Depar'ment as rearranged in 13S1-S2.
and before the metal is poured into moulds it is stirred with an
ii'on rod having a flattened end. The i jrface of the molten metal is
covered with a layer of charcoal to prevent oxidation of (lie copper.
The crucible with its contents is then removed from the furnace
by the aid of a crane and tongs W, and is placed in a cradle M,
T^iicli can be tilted by means of a lianillo D. By the interven-
tion of toothed wheels E, F, G, H, and K acting on a rack the
handle tnrns the crucible on the fulcrum formed by a spindle,
80 that the contents of the crucible may be poured into the moulds
K mounted on a carriage OP, i-unuing on rails Q, Q. The moulds
now in use in London are of such dimensions as to enable bars to
be cast 12 inches Ion" and * inch thick. The width of the bars
varies, according to Ine coin to be jtroduced, from IJ to 2£ inches.
When the metal has solidified in the moulds it is removed, and
the bare are trimmed by the aid of a revolving circular file, their
ends being cut off and returned to the melting pot. Portions of
metal are then cut from certain of the bai-s, and sent to the assay
ilcpartmcnt. The bars are weighed before they pass to the subse-
quent operations of coinage, in order that the amount of metal re-
tained by the crucibles or cairicd into the flues may be ascertained.
Gold biiUion is melted in a similar way, but the crucibles are
smaller, and contain only 1200 oz. Their contents are pouicd by
hand into moulds, one end of the tongs by which the crucible is
grasped being supported by a chain and suspended from the roof.*
In many Continental mints it is very gemrally the ]iractico to
leave the crucible containing the precious metals in ilie furnace,
and to pour the contents into the moulds by the aid of small ladles
of wrought iron lined with clay. I
It has been pointed out in Gold (vol. x. p. 751) that minute;
quantities of certain metals render standard gold cxtiemely brittl»|
and unfit for coinage. If cither the gold bullion or the copper
used as an alloying metal should be impure, brittle bars will b»'
the result. Should this prove to be the case, the bats are re«|
' A new form of furnace devised by M. A. Piat of Paris has recently,
been introduced. In these furnaces the portion which contains tbo]
cruriblo may be detached from the flue, so as to admit of the nioUeili
metal being poured into moulds without removiug the crucible from
the incandescent fuel. Four of such furnaces have been fitted up ld;
the gold melting-house, but have not as yet been used for gold melt-
ing ; in the melting of silver and bronze, however,, they arc known t«'
effect considerable economy in labour, fuel, and crucibles.
MINT
487
UnlHtig
melted and chlorine gas is passed through the molten mass in the
manner described in Gold, vol . i, p. 750.
The engine-room (shown in fig. 1) contains three 60-horse-
power verrical condensing engines, which are provided with Corlis
valves, and are specially devised for meeting the constantly vary-
ing strain to which they are subjected by the machinery, the
whole of which they aro capable of driving. The central engine
acts directly on either or both of the rolling rooms placed on each
side of the engine-house. There is, however, an additional 20-horse-
power compound beam engine usually employed, in connexion with
the pumps of a deep artesian well.
Into one or other of these rooms the bars which have been cast
in the melting-house are brought, and are rolled into strips the
thickness of which depends on the kind of coins to be produced.
Gold is rolled in one room and silver or bronze in the other. The
details of manipulation involved in the conversion of gold, silver,
or bronze bara into coin, however, do, not differ mateiially, and tho
coinage of sovereigns will therefore be taken as typical
Each room contains six pairs of rolls, the diameter of the rolls
varying from 10 to 14 inches. Smaller diameters are employed in
most European mints, but on the other hand the use of very narrow
rolls of far larger diameter has often been suggested, and there
appears to be good ground for the belief that the rigidity of such
rolls would enable strips or fillets of more uniform thickness to be
>'I0. 2. — Furnace Apparatus.
produced than is the case at present. The iron frame CO (fig. 3) is
firmly bolted to the stone D, which rests on a solid foundation EE.
This frame supports the two rolls A, 6, the lower of which B
revolves, bat is not, like the upper, capable of adjustment in a ver-
Fia. S.— Rolls.
tical plane. The upper roll is centred in bearings, and may be raised
or lowered by means of screws connected with toothed wheels F, F,
which are turned by a handle G, both wheels being moved simulta-
neously by worms on the rod H. The bearings of the upper roll ai-e
connected by vertical rods with weights below the level of the floor ;
and, as it rises with the screws, it can thus be readily ac^nsted in a
line e.tactly parallel with the lower roll, at a sufficient distance
from it to admit the bar which is to be reduced to a strip or fillet,
Tho rolls are turned by the shaft XN, the main wheel JI, and
the gearing K, L, 0, P. The sockets r by which the upper roll is
connected with the gearing by the shaft I arc not rigid, as is
the case with the shaft Q of the lower roll, but admit of the adjust-
ment of the roll. The portion of the roll used is determined by a
fuide a little wider than the bar.' Tho rolls throughout this
epartment are driven at the rate of about 32 revolutions in a
minute. The iron frame CC is braced by rods a, s; and blocks
bearing the driving shafts are shown at k, jt, p, p.
The initial thickness of a sovereign bar is |ths of an inch. The ban
are weighed out to the workmen in batches of about sixty bars,
an entire batch being passed through the rolls under precisely ths
same conditions of adjustment. The bars are only slightly reduced!
in width by repeated passages through the rolls, but are successively;
reduced in thickness in tlie fii-st stages of the rolling by iVth of ai^
e"eH
elntha
> In the second rolling room, shown in tho plan on llie rii:ht of the i
honse, the frames and gearing of the i-olls are of newer pattern than those i
6rst room. Id some of the six pairs the bottom rolls revolve and drive the ttppeij
ones. In the pair of " breaking-down " rolls in this room,— tliat is, tho roll br
which the lillets arc first treated, — tho upper roll is stationary, the lower roll
alone revolving. The necessary ''bite" 1^ given to the l^llet, vrhtm Its end IS
Introdoced. by illgbUy turning the upper nil by oieaus of a ratchct-whevl and
lever.
488
MINT
inch, while in the Iai£r stages the reduction in thicknessat each
passage through the rolls is less than -rJ^th "' "" >°<=h, and finally
one or two "spring pinches" arc given to the bars by simply pass-
ing them through the rolls without alteiing the adjustment. The
testing of the lillets, to ascertain whether they are of the accurate
thiclCDess, is effected
by the aid of the gauge
plate (fig. 4), which
consists of two steel
bars set at a low angle
in relation to each
other and graduated „ . „ -n, ^
to xT^th of an inch. Fio. 4.-Gauge Plate.
It mil be evident that the weight of the finished coin depends upon
the thickness of the fillets ; and to show how accurately the rolling
must be performed it may be pointed out that, in the case of the
half-sovereign, a variation of ^^Imtth of an inch above or belovf the
accurate thickness (or a range of roinjtli °^ ^" ii"!h) throws the
coin out of "remedy."
The repeated passage through the rolls is attended by a consider,
able increase of hardness in the metal, and it is therefore in some
cases necessary to anneal the fillets repeatedly during the rolling.
In the case of fillets for sovereigns the annealing may he entirely
dispensed with if the initial thickness of the bars does not exceed
fths of an inch. Fillets for half-sovereigns have only to be annealed
one:;. In some European mints the fillets are annealed frcfiuently ;
in one mint the operation is performed after each passage through
the rolls. The furnace used for the purpose is generally so arranged
as to permit the flame to play over the fillets, which are sometimes
freely exposed to its action, but are more often enclosed in cases or
tubes. Muffle furnaces are frequently used. The furnace used in
the Royal Mint is a simple form of reverberatory furnace. The
final rolling is giveu by a pair of finishing rolls capable of more
accurate adjustment than the "breaking-down" rolls.
The fillets of gold or silver are in some cases, though not alw.iys, Drag
submitted to an appliance known as the drag bench, shown in bench
figs. 5, 6, 7. Its object is to equalize the tiiickness of the fillets by
drawing them between steel cylinder.- '^^" „,„i„ «f ti,» r,ii„t» „...,
The ends of the fillets are
Figs. B, 6, 7. — ^Drag Bench.
first flattened in a little appliance, which need not be described.
The essential feature of the
Biachine now used in the
mint consists of two small
steel cylinders A, A, which
do not revolve, and are
held in position in the
plates D, D by clamp pieces
F, F screwed against them.
The portions of metal may
be adjusted by the aid of
a wheel and screw H (figs.
C, 7), and by small ad-
justing screivs /, /. The
part of the machiuo con-
taining the steel cylinders
>3 fixed at the end of a
long bench, and ^caring at
the other end of tliis bench
drives an endless chain BB
(fig. 6), one link or other of i
which catches the carriage,
shown in plan in fig. &, and
drags it along as soon as
its end / is depressed by
the handle r. The carriage
runs on the wheels d, d.
The drawing of the fillet
C is conducted as follows.
Its flattened end is intro-
duced between the steel
cylinders, and is giasped
l^ the jaws a. The jaws
t«m on the pin c, and while
tho fillet is being dragged
UirouKh tho cylinders the
axle of the wheels d, d tends
to increase the grip of the
jaws by acting on their inclined ends. Directly tho str^ on tho
FlO. 8. — Cutting Machii
fillet is released, the pins i, i and the weight h loosen the jaws and
at the same time raise the end of the carriage so as to ancst its
further progress along the bench. The . carriage is then moved
forward by the handle s untU the jaws enter the hollowed portion
N and grasp another fillet.
Foi-merly — when fillets were rolled from thick bars — this appliance
played a more important part in coining operations than at present
It is now only used for fillets from which sovereigns and half-
sovereigns are to be produced. Before fillets are passed on to the nex t
operation — that of cutting from them the disl;s or blanks destined
to form the coin — they are carefully tested by a skilful workman
called the " tryer," who cuts one or two blanks from tho sides of TiTi^g
each fillet by the aid of a cutter worked by hand. The.'iC blanks
are weighed on a delicate balance against a standard weight, and
tho experience of the operator enables him to determine whether tho
variation from the exact weight will justify his sending the fillets for-
ward to the cutting room. In any case he divides the fillets into
two or more classes for a reason that will bo explained presently. _ ,
The cutters employed in the mint until quite recently were of Cottill
complicated construction, but these have been replaced by a simple blaals.
machine (fig. 8) which, by the revolution of an excentric A, causes
two short steel cylindei'S, mounted on a block of iron 11 suitably
guided, to enter two holes firmly fixed in a plate on the bed of the
machine. Wlien the fillet FF is i
machine. When tiic fillet fi' is ^- r~\r\r-^r\r\r^i^\
interposed between the short cylin- > Lli^PiJiUiULJ}^
dcrsand the holes, the former force £ Q C ./ O OOP
disks of metal through (ho holes, _. .
tlic fillet being advanced at each »• •
stioko of the machine by small gripping rolls C, C, C" actuated by a
ratchet-wheel E, driven from the shaft which bcare the excentric A.
Tlio disks pass down the tube G to a receptacle placed on the floor.
In tho case of very largo silver coins, only one disk is cut iji the
width of the fillet, and in some few mints" disks for gold coin are
also cut in this way, but it is far more usual to cut two disks in
tho width of tho fillet, the position of the cuttere being so arranged
as to remove blanks in the manner shown in fig. 9. In cutting
di.^Ics for bronze coin extreme precision is not necessary, and it hns
thercroro been found possible to obtain five at each stroke of the
machine.
M i ^ T
489
gbnks.
It will be evident that the rough classification of the fillets
according to their thickness, to which reference has already been
made, renders it easy to compensate for slight irregularities in thick-
ness caused by rolling, by employin" cutters of a slightly larger
diameter than the standard size for fillets which are too thin.
The fillets after the removal of the disks present the perforated
appearance shown in fig. 9. The residual metal, called "scissel,"
which amounts to from 25 to 30 percent, of the metal operated upon,
is returned to the melting-house in bundles weighing 180 oz. It
may be mentioned hero that all attempts to cut disks or blanks for
coinage from the ends of rods or cylinders, and thus to avoid the
pi«duction of scissel, have hitherto failed.
The next operation to which the blanks are submitted varies in
different mints. In some, each blank is weighed by hand or by
automatic machinery, and each blank that is too heavy is adjusted
either to an exact weight or to within the remedy prescribed by
law. On the Continent it is very generally the practice to adjust
blanks by the aid of a file, or by a machine that removes a fine
shaving of metal from the surface of the blank. In mints where
mechanical adjustment isadopted there is a tendency to produce
' ' too heavy " blanks in the rolling and cutting departments, as it is
impossible to adjust blanks which are too light'
In the London mint finished coin alooe is weighed, so that ^
blanks after leaving the cutting room pass directly to an edge-roUinit
machine, which thickens the edge of each blank so as to form arm
intended to protect the impression on the finished coin Tlie
operation of edge-rolling is called "marking," and the method of
conducting it varies considerably in difierent mints.
In the Royal Mint the blanks are made to pass in quick succes-
sion, at thp rate of six hundred a minute, between a circular groove
in the face of a revolving steel disk and a groove in a fixed block
placed parallel to the face of the revolving disk. The groove ia
the block exactly corresponds to that on the disk ; and aa tho
distance between the block and the disk is slightly less than
the diameter of the blank submitted to* the operation, tho result ia
that before the blank escapes from the machine its edge has been
thickened. The operation may be varied by admitting the blanks
between a groove in the periphery of a revolving wheel and a groora
in a segmented block, placed at a distance from the wheel rather
less than tho diameter of the blank. The wheel and block may be
either vertical or horizontal.
In some cases the edges of the blanks, at the same time that they
are thickened, receive the impression of a legend, or inscription, or
an ornamental device. Wlien this is tho case the blank is rolled
Fig. 10.
between t-*o planes, one of which is fixed and bears tho device,
while the other has a reciprocating motion imparted to it, or the
edge of the blank receives the impression, which may be either raised
t A description of a machine lued for the adjoatment of hianks wiU he found
In rmgler'i Polirtf^Misehet Journal (1882, ccxl7. 61, pi. C) ; and eome years ago
Mr J. M. Napier devised for the Indian mints a heantiful machine which first
ascertains hov much it is necessary to cut from each blanlc lu order to reduce it
to the standard weight, and then removes tho necessary amount of metai and
no more. The initial cost of such machinery, however, is considerable. In 1849
M. Diereck, director of tho mint In Paris, endeavoured to substitute a chemical
for a n'.echanlcal treatment by submitting the hea^-y gold blanlfs to aqua regia,
which it was anticipated would liring them within the prescribed limits of
accuracy. Tho results were not satisfactory, and the attempt was abandoned.
In 1870 the present chemist of the mint, Professor W. Chandler Roberls, showed
thiit gold alloyed with copper might be removed from heavy blanks with singular
regjlarity by means of a suitable solvent aided by a battery. The blanks are
arranged In a frame of wood and submitted to the action of a solution of cyanide
of potassium, the heavy blanl^s forming the dissolving pole of the battery. Tho
process was not used in the London mint, as It became evident that it could not
Brolitably replace the present system, under which finished coins alone are
•Svciffhed and the manufacture of good coin only is paid for. It was, how(»er,
Introduced into tho Bombay mint in 1670 by the late Mr L. G. Hines, who
extended Its usefulness by transfeiTiog the metal di3£r>lved from the heavy
blanks to blanks which arc too liglit. tlic latter being by this means raised to the
prescribed weight. The process has now fairly talcen its place as an ordinary
operation of coining, and its importance to the mints where it is used may be
gathered from the fact that In the Indian mints no less than 1300 tons of silver
were converted Into coin in one year (1879), so that the a^ving effected by Its
Introduction most be consideiable.
Fig. n.
or sunK, from a collar surrounding the blank in the coining press, as
will be afterwards explained.
Before passing to the coining press the blanks either of gold or innaait
silver are annealed. In many mints the object of the heating is ing tha
not only to soften the blanks before they receive the impression, but o'.nnka.
also to produce a film of oxide of copper on their surface. This is
attained in various ways. In England gold blanks are placed in
cylindrical crucibles of plumbago and covered with a layer of ohai-
coal, heated in a reverberatory furnace, and when the blanks reach
cherry-redness they are cooled by plunging them in water. Tho
thin film of oxide of copper thus formed on the surface of the gold
or silver blanks is readily soluble in dilute sulphuric acid, and the
removal of a small portion of the alloying metal in this way con-
stitutes "blanching" or "pickling" the coin. The method ol
conducting the operation varies somewhat in different mint^
mainly, however, in the strength of the acid used, which varies from
3° to 5° of the hydrometer of Baume. The solution is sometime
heated to 96° to 98° C, while in other cases tho blanks are intro-
duced into the solution while at a red heat. The latter method is,'
however, objectionable, as a dense layer of pure metal is found at tha
surface of the blank which is apt to protect the underiying onde ol
copper from the action of the acid. The blanks are aJtenrards
washed in pure vratcr and dried either in sawdust or in copp«
Tossela heated by steam jackets. Tho object of the process is to?
XVI. — 62
490
HINT
improTc the appearance of the finished coin by removing all traces
of impurity from the surface of the blank. It has, however, been
abandoned in the British mint except in the casa of some of the
smaller silver coins, mainly because the soft sxiperficial layer of
metal wears away with undue rapidity. Certain precautions
suggested in 1869 by Mr Hill, the superintendent of the operative
department, for avoiding oxidation or tarnishing of the metal
during coinage rendered the abolition of the process possible.
Ooinii^' -The blanks receive tlie impression which constitutes thorn coins
pre68. from engraved dies. Each is placed in the lower of two dies, and
the upper die is brought forcibly down upon it. The lateral escape
of the raetal is prevented by a collar which surrounds the blank
while it is being strack. This collar may be either plain or
engraved, and if tlic latter is the case any device or ornament it
may bear will be imparted to the edge of the blank.
The coining presses used in various mints may be divided into
three types : — (1) the screw press worked by atmospheric prcs'-.ure,
(2) the excentric press, and (3) the lever press. The fii'st of these
(see Ency. Brit.^ 8th ed., vol. vii. p. 92) has now been abandoned.
In the excentric press the power is applied to a shaft bearing an
excentric which acts by means of a connecting rod upon a verti-
cal slide holding the die which is brought down on the blank. This
form of press is used in the mint at Constantinople, where the atmo-
spheric screw press is also still retained. Of the third tj^po, the
lever press, there are two modifications, devised respectively by
Thonnelier and by Uhlhorn, The details of the Uhlhorn press have
been improved by Messrs R. Heaton & Sons of Birmingham ; and,
their Euperiority to the old vacuum screw press bavins; been demon-
strated by careful experiments, they have been finally adopted in
the newly arranged mint, which contains fourteen of them. This
press is shown in figs. 10 and 11. It is driven from below the
floor of the press-room by bands which pass over fast and loose
pulleys on the same shaft that bears the fiy-wheel. The loose
pulley, however, ia only used when it is necessary to stop the
machine entirely, as the fly-wheel is permitted to revolve without
imparting motion to the shaft so long as a lever M, worked from
the front of the machine, does not cause the fly-wheel to be con-
nected with the driving wheel by means of two pins. The dies are
placed in the front part of the machine (fig. 10). The lower one is
nrmly fixed to the bed, while the upper is held at A by the upper of
two Jaws F and A', or levers, the fulcra of which are so close together
as almost to coincide, the lower jaw A' bearing the collar which
encircles the blank while it is being converted into a coin ; the
upper Jaw F, A, governed by the weighted lever H shown below the
bed of the machine, has a tendency to rise a sufiicieut distance
to admit the blank between the upper and lower die. A crank B
on the shaft bearing the fly-wheel is connected by a rod C with
the bent lever D, and this bent lever, acting through the toggle
joint and a piece of metal E connected with the jaw that bears the
Fig. 12.
upper die, forces it down, and thus squeezes the blank between the
upper and lower dies. A cam on the crank shaft acting on the
lower of the two lovers G shown below the bed of the machine causes
the loxver jaw A' beai'ing the collar which surrounded the blank
to bo depressed sufiiciently to leave the finished coin freely resting
on the lower die, from wh'^nce it is driven down the shoot N by the
next blank in succession. Coins are produced at rates varying from
CO to 120 a minute, 90 a minute giving the best results. Tho
blanks to bo convrted into coins are placed on the slide J, and tho
advance of each blank iu succession ia regulated by tho rod called
the " layer on " K, tho backv.ard and forward movemetit of which is
also regulated by an excentric on the crank shaft. The details of
thirt part of the machino are shown in plan, fig. 12.
^ut■.>- Tiio last oi»eration before tho finished coin is returned to tho mint
£»t^*' office for issue to the public is the weighing each gold or silver piece
■*'*"**^' separately. This is eliected in the Americt»n and in most Continental
'mints by hand, but in England automatic balances of beaatifut
construction arc employed. They were originally devised for
separating worn pieces from those of current weight, but they are now
employed to distinguish between "light," *'heavy,"and **good"
pieces, the latter alone being permitted to pass into circulation. In
the newly arranged department thirty sucn machines are provided.
Each is driven from overhead shafting by means of gut lines. Tlie
dri\'ing pulleys derive their motion from a small atmospheric
engine, which is found to givj more satisfactory results than would
bo the case if the steam-engine were employed directly. Each
balance is worked by a cone pulley A (fig. 13) by a' gut lino
passing round it from the loose pulleys B, the necessary ten-
sion being imparted to the line by means of a spring C. The
tension of the line is, however, but slight, for if tho action of
the balance is arrested by accident, the cord slides over the cone
pulley A without turning it. It will be obvious that the use of
the cone pulley enables the machino to be driven with varying
degrees of speed. The toothed wheel D is mounted on the spindle
which bears tho driving pulley A, but it acts only througli the
intervention of a friction cneek, which is eo lightly screwed against
the driving wheel that it would cease to act ii the machine should
be accidentally deranged. The wheel D sets in motion the wheels
E, E', E". The cam F, acting on the curved cxiremity of the rocking
frame G, causes the slide H to bring fom-ard one of a scries of coins
(arranged iu th« hopper I) until it rests on the plate J of the balance
beam, qf which beam a portion is shown in an enlarged drawing
above the balance, while the plate that receives the coiji is also shown
in a separate drawing to tho left of tho machine. Another cam K
then comes into play, and enables tho forceps, sho'wn at L, torelea&o
the rod M to which tho balance plate J is attached. Tlie forceps L
serves to keep the rod steady while tho coin is being placed on tlie
plate J. A rod shown at N is then raised by the cam 0, the lowtr
extremity of the rod being kept steady by a pin diding in a hole in
the bottom plate of the balance, and its upper end by a pin which
works into tne central support of the balance beam. At tlio base
of this rod N", and at right angles to it, there is a metallic bar CiSi,
the ends of which pass through stiiTuns in the pendants M and V
from the opposite ends of the beam. The elevation of this horizon-
tal rod by the cam 0 simultaneously releases both ends of the beam,
and the coin placed on the beam plate has then, for the first time,
a direct influiiuce on the beam.. If the coin is "too light" the
counterpoise R iu the cage at the end of the rod P will raise the
coin, and the revolution of the machine then causes part of the cam
K to permit a spring to close" the forceps L and to hold the pendant
M firm. An indicating finger T then falls, and by means of a
horizontal lever UU', which fits into one of three inverted steps on
the bottom of the shoot V, determines over which of three orifices
W, W,W" in the bottom plate of the balance this shoot shall stand.
In the meantime the advance of the slide H brings tho next piece
forward, and displaces the coin which has hitherto occupied the
beam plate J, forcing the coin down the shoot V, and thence through
the orifice W into a receptacle, external to the balance, destined for
the reception of " light coin." If this nest piece should be '*too
heavy " it will not only raise the counterpoise ii but will also elevate
a little wire S, which would otherwise remain undisturbed on a
support. This little wire represents tho "working remedy" for
the particular denomination of coin in question, which, for safet},
is Irss by -y^th of a grain tlian the remedy permitted by law. Tht
undue weight of the *' heavy coin " will depress the right end of tlu
t.^lanco beam and its pendant M to tho lowest possible point, an«l
the indicating finger T will, in this case, determine that the rou
UU' s'tall occupy the lowest step of the shoot V, which ^n^l conse-
quently stand over the orifice W in the bottom plate of the balance
which communicates with the receptacle for the "heavy" coins,
and the heavy coin on tho beam plate will be driven do-mi the
slioot by the next coin in succession. If the coin which is nex^
brought fon\'aa'd by the slide II should bo a "good" oue, that is,
if it 13 within the working "rcmcdy,"it3 action will lie as follows.
It maybe slightly heavier than tho counterpoise, but not sufiiciently
heavy to lift both the counterpoise and the remedy wire. The
balance beam consequently remains approximately horizontal, and
tho indicating finger T will cause the rod UU' to strike the centre
step of tho shoot V, which will then stand over tho central orifice AV
in tho bed plate which communicates with a rtoeptacle for "goorl"
coins, into which the coin will find its way, as soon as it ia ai*ivci:
from tho beam plate by tho next coin of tho series. It will be
evident that this excellent appliance both weighs and classifies th<;
coins. About twenty-three coins are passed through it in a minuta
In order to show the importance of extreme accuracy in weighing,
it maybe pointed out that, althongh by tlie Coinage Act of 1870 th-
"iTmedy or allowed variation abovt or below the standard weight
of a sovereign is only \\,\\ of a grain, yet in a million stcriing o'
sovereigns the ditfcrcnco between tho least and the greatest weighs
the law allows would be no less than £3244.
Tlie manufacture of coin 13 not the only work whioh is
performed in the Koytil Mint. AU medals i^ued to the
MINT
491
araiy and navy, us well as those given by the Eoyal
Society and the university of London and some others,
are struck in the mint, and their preparation forms a
considerable part of the work of the die department.
Since 1874 the clasps and bars for the medals have also
been manufactured in the mint, whence they have been
issued completely mounted. Another operation, not con-
nected with the coinage, which is performed in the mint
is the assiy of the " diet " or metal scraped from the gold
and silver plate manufactured at Sheffield and Birmingham
under the direction of the warden of the standard of
wrought plate for those towns. By Act of Parliament it
is directed that this shall be brought once in each year to
the mint to be assayed by the " king's assay master "
under the supervision of an officer appointed by the lords
of the Treasury.
Fic. 13. — Aotomatic Balance.
The gold coin in circulation in Great Britain is esti-
mated at £100,000,000. It may be well to add the
follo\ving table, which gives the value of the gold and
silver coinages of four of the most important foreign
countries, in two recent years : —
1880.
IfSl.
Gold. I Silver.
Gold. 1 SilTcr.
UniUd States
Germany
Austria
£12,461,655:£5,4Sl,94l!£19,370,178'£5,5S7,84d
1,332,430 ... 326,8371
493,605 1,674,712 485,9991 1,805,734
83,646J 259,910|
£14,287,690 £7,150,653 £20,266, 66o| £7,653, 484!
The value of the gold coinage of the American mints
during the fiscal year ending June 1882 amounted to
$89,413,447-50, — being greater than that of any previous
year in their history. (w. c. E. — R. A. H.)
MINT, botanically Mentha, a genus of labiate plants,
oopprising about twenty species of perennial herb.s, widely
cbstributed throughout the temperate and sub-tropical
portions of the globe. All the species are furnished with
square stems, opposite, aromatic leaves, and creeping roots.
The flowers are arranged in axillary cymes, which either
form separate whorls or are crowded together into a terminal
spike. The corolla is usually small, and of a pale purple or
pinkish colour ; it has four nearly equal lobes, and encloses
two long and two short stamens. Great difficulty is
experienced by botanists in discriminating the species of
this genus by reason of the occurrence of a large number
of intermediate forms, nearly three hundred of which have
been named and described. Many of these varieties are
permanent in consequence of being propagated by stolons.
In Britain nine of the recognized species are indigen-
ous. Mentha viridis, L., or Spearmint, grows in marshy
meadows, and is the species commonly used for culinary
purposes ; it is distinguished by its smooth, sessile leaves
and lax tapering flower-spikes. Mentha sylveslris, 1., or
Horsemint, chiefly differs from the above in its coarser
iabit and hairy leaves, which are silky beneath, and in its
denser flower-spikes. This plant is supposed to be the mint
of Scrfpture, as it is extensively cultivated in the East, and
is much used in cookery; it was one of the bitter herbs
with which the paschal lamb was eaten. M. rotundifoli-a
resembles the last in size and habit, but is readily distin-
guished by its rounded wrinkled leaves, which are shaggy
beneath, and by its lanceolate bracts. The last two species
usually grow on damp waste ground near roadsides. M.
aquatica, or Capitate Mint, grows in ditches and by the
side of streams, and is easily recognized by its rounded
flower-spikes and stalked hairy leaves. M. Piperita, or
Peppermint, has stalked smooth leaves and an oblong
obtuse terminal spike of flowers ; it is extensively culti-
492
M I N — M I R
■sated for its volatile oiL M. pratensis belongs to a group
of m'"t3 which, unlike the foregoing, have the flowers
arranged in axillaiy whorls and never in terminal spikes ;
it othersvise bears some resemblance in foliage and halit
to M. viridis. if. saiiva, the Whorled Hairy Mint, growsi
by damp roadsides, and M. arvensis in cornfields ; they
are distinguished from M. pralaisis by their hairy stalked
leaves, which in M. arvensis are all equally large, but in
M. saliva are much smaller towards the apex of the stem.
M. Pulcgium, commonly kno\vn as Pennyroyal, more rarely
as Flearmint, has small oval obtuse leaves and 'flowers in
axillary' whorls, and is remarkable for its creeping habit
and peculiar odour. It differs from all the mints above
described in. the throat of the calyx being closed with hairs.
It is met with in damp places on grassy common*, and forms
a well-known domestic remedy for female disorders.
All the plants of the genus Mentha abound in a volatile
oil, which is contained in small receptacles having the
appearance of resinous dots in the leaves and stems. The
odour of the oil is similar in several species, but is not dis-
tinctive, the same odour occurring in varieties of distinct
species, while plants which cannot be distinguished by any
botanical character possess the same odour. Thus 'the
peppermint flavour is found in 31. Piperita, in M. incana,
and in Chinese and Japanese varieties of M. arvensis. Other
forms of the last-named species growing in Ceylon and Java
have the flavour of the common garden mint, M. viridis,
and the same odour is found to a greater or less degree
in if. Sj/ivestris, if, rotundifolia, and if. canadensis. A
bergamot scent is met with in a variety of if. aquatica and
in forms of other species. Most of the mints may be found
in blossom in August.
The name mint is also applied to plants of other, genera,
Jfonarda punctata being called Horsemint, Pycnanthemum
linifolium, Mountain Mint, and Nepeta Caiaria, Catmint.
MINTO, SiE Gilbert Elliot, Fiest Eakl of (1751-
1814), was descended from an old border family, the
EUiots of Minto, and was bom at Edinburgh, April 23,
1751. His father. Sir Gilbert Elliot, was a member of the
administration of Pitt and Grenville, and is spoken of by
Horace Walpoleas "one of the ablest men in the House of
Commons." Young Elliot was educated by a private tutor,
with whom at the age of twelve he went to Paris, where
David Hume, who was then secretary of the embassy,
undertook, from friendship to his father, the special charge
of superintending his studies. After spending the winters
of 1766 and 1767 at Edinburgh University, Elliot entered
Oxford. On quitting the university he became a member
of Lincoln's Inn, and was in 1774 called to the bar. He
entered parliament in 1776, the year of his father's death.
Although he gave a general support to Lord North's
administration, he from the beginning occupied an inde-
pendent position, and in 1782 supported the address of the
Commons against an offensive war with America. From
this time he became a declared follower of Fox and
Burke, with the latter of whom he gradually came to be
on terms of great intimacy. He was created Baron Minto
in 1797, and after filling several diplomatic posts with great
success became in 1807 governor-general of India. The
character and events of his rule in India are described
in vol. xii. p. 805. He was created Earl of Minto and
Viscount Melgund in 1813. He returned to England in
1814, and died on Juno 21st of that year.
Soe Life and Letters of Sir Oilbert Elliot, first Earl of Mint),
from 1751 to 1806, 1874 ; and Life and Letters, 1807-14, 1880. Sco
.llso MiRABEAU.
MINUCIUS FELIX, Marcts, one of the earliest, if not
the earliest, of the Latin apologists for Christianity. Of
his personal history nothing is known, and even the date
»t which he wrote can be oi".ly approximately ascertained.
Jerome {De Vir. III., 58) speaks of him as "Roma
insignis cauisidicus," but in this he is probably only
imj^roviug on the e::prC5sion of Lactanttus (/»is<. Div., v. 1)
who f;o'i.lis of him as " non ignobilis inter causidicos loci."
He is now exclusively known by his Octavius, a dialogue
on Christianity between the pagan Cscilius NataUs' and
the Christian Octavius Januarios, a provincial solicitor,
the friend and fellow-student of the author. . The scene is
pleasantly and graphically laid on the beach at Ostia on a
holiday afternoon, and the discussion is represented as
arising out of the homage paid by Cscilius, in passing, to
the image of Serapis. His arguments for paganism, which
proceed partly upon agnostic grounds, partly upon the
inexpediency of disturbing long-established religious beliefs,
partly upon the known want of culture in Christians, the
alleged indecency of their worship, and the itihercnt
absurdity of their doctrines, are taken up seriatim !.y
Octavius, with the result that the assailant is convinced,
postponing, however, the discussion of some things neces-
sary for perfect instruction to a future occasion. The form
of the dialogue, modelled on the De Natura Deorum and
De JDivinatione of Cicero, shows much care and ability, and
its style is on the -whole both vigorous and elegant if at
times not exempt from something of the affectations of the
age. If the doctrines of the Divine unity, the resuiTection,
and future rewards and punishments be left out of account,
the work has less the character of an exposition of
Christianity than of a philosophical and ethical polemic
against the absurdities of crass polytheism. Christolcgy
and the other metaphysics of distinctively Christian
theology are entirely passed over, and the canonical
Scriptures are not quoted, hardly even alluded to.
The Octavius is admittedly earlier than Cyprian's De Idolomm
Vanitate, which borrows frmm it ; how much earlier can be deter-
mined only by settling the relation iu which it stands to Tertnlliau'a
Apologclicum. "The argument for the priority of Minuciua liaa
been most exhaustively set forth by Ebert ( " TertuUians Verhalt-
nis3 zu Minucius Felix," in vol. v. of the philolos;ico-hisiorical
series in Ahhandl. d. KSnig. Sdchs. Gesdlsch. dcr Wissenxhaflfn,
1S68), who has been followed by Teuffel {Mom. Lit., sec. 308), Eein-
(Celsus' Wahres Wort, 1873), Kuhn, and other scholars. The
opposite view is ably maintained by Professor Salmon ("Minncins
Felix" in Smith's Diet. Christ. Bicgr., 1882). ' The Octavius was
fii-st-printed (Rome, 1643) as the eighth book of Aruobius Adv.
Gerties ; Balduinus (Heidelberg, 1500) first assigned it to its proper
author. There have been numerous subsequent editions, the best
being that of Halm in the Corp. Scriptor. Eccl. Lat. (Vienna, 1867).
Sec Kuhu's monograph, Dcr Octavius dcs Minucius Felix (1882).
MINUET (Fr. ilenuet, from [pas] mentis), a very grace-
ful kind of dance, consisting of acoupee, a high step, and
a balance. Its invention is universally ascribed to the
inhabitants of Poitou. The melody begins with the down
beat, and contains three crotchets in a bar. The music is
made up of two strains, which, from being repeated, are
called repj'ises, each consisting of eight or more bars, but
very rarely of an odd number. Walther speaks of a minuet
in LuUy's opera of Roland, each strain of which contains
ten bars, the sectional number being five, — a circumstance
which renders it very difficult to be danced ; but Luily's
system of phrasing was remarkably irrtgidar. ■ Modern
instrumental composers have introduced into their sym-
phonies and quartetts, <fcc., minuets of rapid movement
and fanciful character, followed by supplementary strains
(called trios) in a different style. Some of these composi-
tions bear but very slight resemblance to the older forms ;
and many of them begin \vith the third beat in the bar.
The finest minuets we possess are those in Handel's Samson
and Mozart's Don Giovanni.
MIRABEAU, HoNORi Gabriel Riqueti, Comtb dk,
(1749-1791), one of the greatest statesmen and orators
' This nnmo occurs in six inscriptions of the years 211-217 found at
Const.intino (Cirta), North Africa (C. /. L., vol. viii.).
MIKABEAU
49.2-
France has ever produced, was bom at Bigaon, near
Nemours, on March S, 1749. M. de Lom^nie has shown
that the family of Eiquet or Riqueti came originally from the
little town of Digue, that they won wealth and municipal
honours as merchants at Marseilles, and that in 1570 Jean
Riqueti bought the chateau and estate of Mirabeau, which
had up to that time belonged to the great Provenjal family
of Barras, and took the title of esquire a few years later.
In 1685 Honors Eiqueti obtained the title of Marquis de
Mirabeau, and his son Jean Antoine brought honour to it.
He served with distinction through all the later campaigns
of the reign of Louis XIV., and especially distinguished
himself in 1705 at the battle of Cassano, where he was so
severely wounded in the neck that he had ever after to wear
a silver stock ; yet he never rose above the rank of colonel,
owing to his eccentric habit of speaking unpleasant truths
to his superiors. On retiring from the service he married
Fran^oise de Castellane, a remarkable woman, who long
survived him, and he left at his death, in 1737, three sons
— Victor, Marquis de Mirabeau (see next article), Jean
Antoine, Bailli de Mirabeau, and Comte Louis Alexandre de
Mirabeau. The great Mirabeau was the elder surviving
son of the marquis. When but three years old he had
a virulent attack of confluent small-pox which left his
face for ever disfigured, and contributed not a little to
nourish his father's dislike to him. His early education
was conducted by Lachabeaussi6re, father of the better
known man of letters, after which, being like his father
and grandfather destined for the anny, then the only
profession open to young men of family, he was entered
at a pension militaire at Paris, kept by an AbbiS Choquart.
Of this school, which had Lagrange for its professor of
mathematics, we have an amusing account in the life of
Gilbert Elliot, first earl of Minto, who with his brother
Hugh, afterwards British minister at Berlin, there made
the acquaintance of Mirabeau, an aoquaintance which
soon ripened into friendship, and to which Mirabeau in
later life owed his introduction into good English society.
On leaving this school in 1767 he received a commission
in the cavalry regiment of the Marquis de Lambert, which
his grandfather had commanded years before.' He at once
began love making, and in spite of his ugliness succeeded
in winning the heart of the lady to whom his colonel was
attached, which led to such scandal that his father obtained
a lettre de cachet, and the young scapegrace was imprisoiied
in the isle of Rh6. The love affairs of Mirabeau form
quite a history by themselves, and a well-known history,
owing to the celebrity of the letters to Sophie ; and the
behaviour of the marquis in perpetually imprisoning his
son is equally well known, and as ividely blamed. Yet it
may be asserted that until the more durable and more
reputable connexion with Madame de Nehra these love
episodes were the most disgraceful blemishes in a life
ather\*'i3e of a far higher moral character than has been
commonly supposed. As to the marquis, his use of lettres
de cachet is perfectly defensible on the theory of the exist-
ence of lettres de cachet at all They were meant to be
used (see Lettres de Cachet) by heads of families for
the correction of their families, and Mirabeau, if any son,
surely deserved such correction. Further, they did have
the effect of sobering the culprit, and the more creditable
part of his life did not begin till he left Vincennes.
Anrabeau, it may be remarked at once, was not a states-
man of the Alcibiades type, and he did not develop his
great qualities of mind and character until his youthful
"excesses were over. These will be passed over as rapidly
as possible, for it was not till 1781 that the qualities which
made him great began to appear.
On being released from his first imprisonment, the young
count, who had always intended to continue his military
career, obtained leave to accompany as a volunteer thff
French expedition which was to effect the reduction of
Corsica. The conquest was one of sheer numerical
strength, for the whole population was on the side of
Paoli, and Mirabeau, perceiving the value of public opinion,
is said to have written a treatise on the oppression tlia
Genoese had formerly exercised over the island, which the
Govenmient was ready to publi.sh had not the Marquis de
Mirabeau thought fit to destroy it because of its divergence
from his own philosophical and economical views. For his
services in Corsica Mirabeau was made a captain of
dragoons, though not in any particular regiment, and on his
return his father endeavoured to make use of the literary
ability he had shown for the advancement of his own
economical theories. He tried to keep on good terms with
his father, though he could not advocate all his ideas, and
even went so far in 1772 as to marry a rich heiress, a
daughter of the Marquis de Marignane, whose alliance his
father had procured for him. He did not live happily
with her, and in 1774 was ordered into semi-exile in the
country, at his father's request, where he wrote his earliest
extant work, the JEssai eur le JDespoiisme. His violent dis-
position now led him to quarrel with a country gentleman
who had insulted his sister, and his serai-exile was changed
by lettre de cachet into imprisonment in the Chateau d'If.
In 1775 he was removed to the castle of Joux, to which,
however, he was not very closely confined, having full
leave to visit in the town of Pontarlier. Here he met
Marie Therfese de Monnier, his Sopliie as he called her, a
married woman, for whom he conceived a violent passion.
Of his behaviour nothing too strong can be said : ho was
introduced into the house as a friend, and betrayed his
trust by inducing Madame de Monnier to fall in love with
him, and all his excuses about overwhelming passion only
make his conduct more despicable. The affair ended by his
escaping to Swtzerland, where Sophie joined hkn ; they
then went to Holland, where he lived by hack-work for the
booksellers ; meanwhile Mirabeau had been condemned to
death at Pontarlier for rapt el vol, of which he was certainly
not guilty, as Sophie had followed him of her own accord,
and in May 1777 ho was seized by the French police, and
imprisoned by a lettre de cachet in the castle of Vincennes.
There he remained three years and a half, and witli his
release ends the first and most disgraceful period of his life.
During his imprisonment he seems to have learnt to control
his passions from their very e.xhaustion, for the early part
of his confinement is marked by the indecent letters to
Sophie (first published in 1793), and the obscene Erotica
Biblioii and Ma Conversion, while to the later months
belongs his first political work of any value, the Lettres
de Cachet. The Essai sur le Despotisme was an ordinary
but at times eloquent declamation, showing in its illustra^
tions a wide miscellaneous knowledge of history, but the
Lettres de Cachet exhibits a more accurate knowledge of
French constitutional history skilfully applied to an
attempt to show that an existing actual grievance was not
only philosophically unjust but constitutionally illegal It
shows, though still in rather a diffuse and declamatory
form, that application of wide historical knowledge, keen
philosophical perception, and genuine eloquence to a
practical purpose which was the great characteristic of
Mirabeau, both as a political thinker and as a statesman.
With his release from Vincennes begins the second period
of Mirabeau's life. He found that his Sophie was an ideal-
ized version of a rather common and ill-educated woman,
and she speedily consoled herself with the affection of a
young officer, after whose death she committed suicide.
Mirabeau first set to work to get the sentence of death still
hanging over him reversed, and by his eloquence not only
succeeded but got M. de Monnier condemned in the costs of
494
MIKAHEAU
the wliole law proceeJiugs. From Pontarlier he went to
Aix, where he ckimed the court's order that his wife should
return to him. She naturally objected, but his eloquence
would have won his case, even agaiust Portalis, the leader
of the Ai'y bar, had he not in his excitement accused his
wife of infidelity, on which the court pronounced a decree
of separation. He then with his usual impetuosity inter-
vened in the suit pending between, his father and mother
before the parlement of Paris, and so violently attacked
the ruling powers that he had to leave France and again go
to Holland, and try to live by literary work. About this
time began his connexion with Madame de Nehra, which
sweetened the ensuing years of toil and brought o^t the
better points of his character. She was the daughter of.
Zwier van Haren, a Dutch statesman and political writer,
and was a woman of a far higher type than Sophie, more
educated, more refined, and more capable of appreciating
Mirabeau's good points and helping him to control his
passions. With her the lion became a lamb, and his life
was strengthened by the love of his jyetite horde, Madame
de Nehra, her baby son, afterwards Lucas de Jlontigny,
and his little dog Chico. After a period of work in
Holland he betook himself to England, where his treatise on
Leltres de Cachet had been much admired, and where he
was soon admitted into the best Whig literary and political
society of London, through his old schoolfellow Gilbert Elliot,
who had now inherited his father's baronetcy and estates,
and become a leading Whig member of parliament. Sir
Gilbert introduced him freely, but of all his English friends
none seem to have been so intimate with him as Lord Lans-
downe, and Mr (afterwards Sir Samuel) Romilly. The
latter became particularly attached to him, and really
understood his character ; and it is strange that his remarks
upon Mirabeau in the fragment of autobiography which
he left, and Mirabeau's letters to him, should have been
neglected by French writers. Romilly was introduced to
Jlirabeau by D'lvernois, and readily undertook to translate
the Consideration on ike Order of Cincinnaius. Konully
writes thus of him in his autobiography : —
" The count was difficult enough to please ; he was sufficiently
impressed with tlie beauties of the original. He went over every
part of the translation with nic, observed on every passage in which
jusfite was not done to the thought or the force of the expression
lost, and made many useful criticisms. During this occupation
we had occasion to see one another often, and became very inti-
mate ; and, as he had read nnich, had seen a great deal of the world,
was acquainted with all the most distinguished persons who at that
time adorned either the royal court or the republic of letters in
Fr.Tjice, had a great knowledge of French and Italian literature, and
possessed very good taste, his conversation was e.^trei\iely interest-
ing and not a little instructive. I had such frequent opportunities
of seeing him at this time, and afterwards at a much more import-
ant period of his life, that I think his character was well known
to me. I doubt whether it has been so well known to the world,
and I am convinced tliat great injustice has been done him. This,
indeed, is not surprising, wiien one considcis that, from the first
moment of his entering upon the career of au author, he had been
altogether indifferent how numerous or how powerful might be the
enemies ho should provoke. His vanity was certainly excessive ;
but I have no doubt that, in his public conduct as well as in his
writings, he was desirous of doing good, that his ambition was of
the noblest kind, and that he proposed to himself the noblest ends.
}fe was, however, like ma\iy of his countrymen, who weve active in
the calamitous'KcvoIution which afterwards took place, not suffi-
ciently scrupulous about the means by which those ends were to be
accomplished. He indeed to some degree professed this ; and more
than once I have heard him say that there were occasions upon
which Ma petite morale (itait cnncniie do la grande.' It is not sur-
)irising that with such maxims as these in his mouth, unguimled
ill his expressions, and careless of his reputation, he sliould have
afforded room for the circulation of many stories to his disaJvan-
tigo. Violent, impetuous, conscious of the superiority of his
talents, and the dcckred enemy and denouncer of every species of
tyianny and oppression, ho could nnt fail to shock tlio prejudices,
to opposie the interests, to excite the jealousy, and to wound tho
piido of many descriptions of poraons. A mode of refuting his
works, open to the basest and vilest of mankind, was to represent
him as a monster of vice and profligacy. A scandal once set on
foot is strengthened and propagated by many, who have no nialica
against tho object of it. They delight to talk of what is extraordi-
nary ; and what more extraordinary than a person ao admirable for
his talents and so contemptible for his conduct, professing in faJB
writings principles so excellent and in all the offices of public and
private life putting in practice those which are so detestable ? J
indeed possessed demonstrative evidence of the falsehood of some of
the anecdotes which by men of high character were related to hia
prejudice." — Life of Sir S. Jiomilli/, vol. i. p. 58.
This luminous judgment, the best that is extant on the
character of Mirabeau, deserved to be quoted at length ; it
must be noted that it was wxitten by a man of acknow-
ledged purity of life, who admired Mirabeau in early life,
not when he was a statesman, but when he was only a
struggling literary man. This close association with
Romilly, and his friends Baynes, Trail, and AVilson, does
credit to Mirabeau, and must have helped that moral
revolution against his passions which was passing within
him. He was a warm friend, and first made Romilly
acquainted with Lord Lansdowne, and tried to get him a
seat in parliament. Lord Lansdowne was himself an
extraordinary man, and the first of the new AVhigs might
well feel 'sympathy with the statesman of the French
Revolution. The CoTisiderations &ur I'ordre de Cincinnatus
which Romilly translated was the only important work
Mirabeau wrote in the year 1785, arid it is a good speci-
men of his method. He had read a pamphlet published in
America attacking the proposed order, which was to form
a bond of association between the officers who had fought
in the American War of Independence against England ;
the arguments struck him as true and valuable, so he
rearranged them in his o^vn fashion, and rewrote them in
his own oratorical style. He soon foiuid such work not
sufficiently remunerative to keep his "petite horde" in
comfort, and then turned his thoughts to employment from
the French foreign office either in wTiting or in diplomacy.
He first sent Madame de Nehra to Paris to make his peace
with the authorities, in which she was completely successful,
and then returned himself, hoping to get employment
through an old literary coUaborateur of his, Durival, who
was at this time director of the finances of the department
of foreign affairs. One of the functions of this official was
to subsidize political pamphleteers, and Mirabeau had
hoped to be so employed, but he ruined his chances by a
series of financial works. On his return to Paris he had
become acquainted with Clavieres, a Genevese exile, who
was minister of finance during the Revolution, and lyho
now introduced him to a banker named Panchaud. From
them he heard plenty of abuse of stock-jobbing, and seizing
their ideas he began to regard stock-jobbing, or agiotage, as
the source of all evil, and to attack in his usual vehement
style the Banque de St Charles and the Compagnie dcs
Eaux. This was at least disinterested on his part, for.
while his supporters were poor, tho bankers he attacket!
were rich, and would gladly have bought his silence ; but
Mirabeau, though ever ready to take money for what he
wrote, never sold his opinions, or wrote what ho did not
really believe. The very eloquence of his style rests upon
the enthusiastic conviction that he himself was right, and
those who differed from him were stupidly and wilfully
wrong. This last pamphlet brought him into a contro-
versy with Beaumarchais, who certainly did not get the
best of it, but it lost him any chance of literary employ-
ment from Government. However, his ability was too
great to be neglected by a great minister such as M. de
Vcrgennes undoubtedly was, and after a preliminary tour
in the early spring of 178G he was despatched in Jimo
1786 on a secret mission to the court of Prussia, from
which he returned in January 1787, and of which Le gave
a full account in his Hiaioire Secrete de la Cour de Berlin.
MIRABEAU
496
The months he spent al Berlin were important or.ea in the
history of Prnssia, for in them Frederick the Great died.
The letters just mentioned show clearly what Mirabeau did
and what he saw, and equally clearly how unfit he was to
be a diplomatist ; for, with all his knowledge of men and
his influence over them, he thought (and showed he
thought) too much of himself ever to be able to surprise
their secret thoughtj and intentions. He certainly failed
to conciliate the new king Frederick William ; and thus
ended Mirabeau'a one attempt at diplomacy. During his
journey he had made the acquaintance of a Major Mauvillon,
whom he found possessed of a great number of facts and
statistics \nth regard to Prus-sia ; these he made use of in
a great work on Prussia published in 1788, as Romilly
says, to show that he could write more than a fugitive
pamphlet. Uut, though his Monarchie Prumenne gave
him a general reputation for historical learning, he had in
this same year lost a chance of political employment. He
had offered himself as a candidate for the office of secretary
to the Assembly of Notables which the king had just con-
vened, and to bring his namo before the public published
another financial work, the Denonciaiion de ["Agiotage,
dedicated to the king and notables, which abounded in
such violent diatribes that he not only lost his election, but
was obliged to retire to Tongres ; and he further injured his
prospects by publishing the reports he had sent in during
his secret mission at Berlin. But 17S9 was at hand; the
states-general was summoned ; Mirabeau's period of pro-
bation was over, and he was at last to have that oppor-
tunity of showing his great qualities both as statesman-
and orator on a worthy arena.
On hearing of the king's determination to summon
the states-general, Mirabeau started for Provence, and
offered to assist at the preliminary conference of the
noblesse of his district. They rejected him ; he appealed
to the tiers etai, and was returned both for Aix and for
Marseilles. He elected to sit for the former city, and was
present at the opening of the states-general on May i,
1789. From this time the record of Mirabeau's life forms
the best history of the first two years of the Constituent
Assembly, for at every important crisis his voice is to bo
heard, though his advice was not always followed. It is
impossible here to detail minutely the history of these two
eventful years ; it mil be rather advisable to try and
analyse the manner in which Mirabeau regarded passing
events, and then shoiv how his policy justifies our analysis.
Mirabeau pos-ses-sed at the same time great logical
acuteness and most passion ite enthusiasm ; he was there-
fore both a statesman and an orator, and the interest of
the last two years of his life lies mainly in the gradual but
decided victory of the statesmanlike and practical over the
impulsive and oratorical qualities. From the beginning
Mirabeau recognized that government exists in order that
the bulk of the population may pursue their daily work in
peace and quiet, and that for a Government to be successful
it must bo strong. In this practical view of the need of a
strong executive lies one of Mirabeau's greatest titles to the
name of statesman. At the same time he thoroughly com-
prehended that for a Government to be strong it must be
in harmony with the wishes of the majority of the people,
and that the political system of Louis XIV. was now fall-
ing for lack of this. He had carefully studied the English
constitution in England under the guidance of such men
as Lord Lansdowne, Sir Gilbert Elliot, and Romilly, and
■appreciated it with the wise approval of its powers of ex-
j^nsion which characterized the new Whigs, and not with
the blind admiration of Burke. He understood the key-
notes of the practical success of the English constitution
to be the irresponsibility of the king, the solidarity of the
ministers, and the selection of the executive from among
the majority of the representatives of tho country ; and he
hoped to establish in France a system similar in principle,
but without any slavish imitation of the details of the
English constitution.
In the first stage of the history of the states-general
Mirabeau's part was very great. He was soon recognized
as a leader, to the chagrin of Mounier, because he always
knew his own mind, and v,as prompt at emergencies. To
him is to be attributed the successfid consolidation of the
National Assembly, its continuance in spite of De Brez4 and
the carpenters, and the address to the king for the with-
drawal of the troops assembled by De Broglie. When the
taking of the Bastille had assured the success of the
Revolution, he was the one man who warned the ^Vssembly
of the futility of passing fine-sounding decrees and the
necessity for acting. He declared that the famous night
of August 4 was but an orgy, giving the people an
immense theoretical liberty while not assisting them to
practical freedom, and overthrowing the old regime before
a new one could be constituted. Still more did he show
his foresight when he attacked the dilatory behaviour of
the Assembly, which led to the catastrophes of the 5th and
6th October. He implored the Assembly to strike while
the iron was hot, and at once solve in a practical maimer
the difficult problems presented by the abolition of
feudalism. But the Assembly consisted of men inexperi-
enced in practical politics, who dreamed of dravring up an
ideal constitution preluded by a declaration of rights in
imitation of the Americans; and for two months the
Assembly discussed in what words the declaration should
be expressed, while the country vras in a state of anarchy,
declaring old laws and customs abolished and having no
new ones to obey or follow, disowning the old adminis-
trative system and having no new one yet instituted, while
Paris was starving and turbulent, and the queen and her
friends planning a coimter-revolution. The result of these
two months' theorizing was the march of the women to
Versailles, and the transfer of the king to Paris. Mirabeau
now saw clearly that his eloquence would not enable him
to guide the Assembly by himself, and that he must there-
fore try to get some support. He ■wished to establish a
strong ministry, wliich shoidd be responsible like an
English ministry, but to an assembly chosen to represent
the people of France better than the English House of
Commons then represented England. He first thought of
becoming a minister at a very early date, if we may believe
a story contained in the Mhnoires of the Duchesse
d'Abrantes, to the effect that in May 1789 the queen tried
to bribe him, but that he refused to be bribed to silence,
and expressed his wish to be a minister. The indignation
^^'ith which the queen repelled the idea may have been
the cause of his thinking of the Due d'Orleans as a possible
constitutional king, because his title would of necessity bo
parliamentary. But the weakness of Orleans was too
palpable, and in a famous remark Mirabeau expressed his
utter contempt for him. He also attempted to form an
alliance with Lafayette, but the general was as vain and
as obstinate as Mirabeau himself, and had his own theories
about a new French constitution. Slirabeau tried for a
time, too, to act with Necker, and obtained tlTe sanction of
the Assembly to Keeker's financial scheme, not because it
was good, but because, as he said, "no other plan was
before them, and something nmst be done."
Hitherto weight has been laid on the practical side of
Mirabeau's political genius ; his ideas with regard to tlia
Revolution after the 5th and 6th October must now be
examined, and this can be done at length, thanks to the
publication of Mirabeau's correspondence with La Marck, a
study of which is indispensable for any correct knowledge
of tho history of the Revolution between 1789 and 1701.
496
M I R'A BEAU
The Comte dc la Marck was a Flemish lord of the house of
Aromberg, who had been proprietary colonel of a regiment
in the service of France; he was a close frien^ of the
gneen, and had been elected a member of the states-
general. His acquaintance with Mirabeau, commenced in
1788, ripened during the following year into a friendship,
which La Marck hoped to turn to the advantage of the
court. After the events of the 5th and Gth of October he
L-onsiilted Mirabeau as to what measures the king ought to
take, and Mirabeau, delighted at the opportunity, di-ow up
an admirable state-paper, which was presented to the king
by Monsieur, afterwards Louis XVIII. The whole of this
Memoire should be read to get an adequate idea of Mira-
beau's genius for uolitics ; here it must be merely sum-
marized.
Tlie main position is tliat the king is not free in Paris ; ho must
ilierefore leave Paris and appeal to France. " Paris n'eu veut que
Targcnt; les provinces deraandent des lois." But where must the
king go? "Se retirer i Jletz on siu- toute autre froutih-e serait
declarer la guerre h. la nation et abdiquer le trone. Un roi qui est la
seule sauvegarde de son peupio ne I'uit point devant son peuplo ;
il le prend pour juge de sa couduite et de scs principes." He must
tJien go towards the interior of France to a provincial capital, best
of all to Rouen, and there he must appeal to the people and summon
a great convention. It would be ruin to appeal to the noblesse, as
the queen advised : ** un corps de noblesse n'est point une armee,
qui puisse combattre," When this great convention met, the
king must show himself ready to recognize that great changes have
f.iken place, that feudalism and absolutism have for ever disappeared,
and that a new relation between king and people has arisen, which
must be loyally observed on both sides for the future. " II est
certain, d'aillcurs, qu'il faut une grando revolution pour sauver le
royaume, que la nation a des droits, qu'elle est en chemiu de les
reconvrer tons, et qu'il faut non seuleraent les retablir, raais les con-
BoUder." To establish this new constitutional position between
king and poojde would not be difficult, because " I'indivisibilite du
nionaraue ct du peuple est dans le occur de tous les Franjais ; 11
faut qiTelle e.^ste dans Taction et le pouvoir."
Such was Mirabeau's programme, which he never
diverged from, but which was far too statesmardike to be
utKlerstood by the poor king, and far too positive as to the
altered condition of the monarchy to be palatable to the
queen. Mirabeau followed up his Memoire by a scheme
of a great ministry to cont9,in all men of mark, — Necker
as prime minister, "to render him as powerless as he is
mcapable, and yet preserve his popularity for the king,"
the archbishop of Bordeaux, the Due de Liancourt, the Due
de la Rochefoucauld, La Marck, Talleyrand bishop of
Autun at the finances, Mirabeau without portfolio, Target
mayor of Paris, Lafayette generalissimo to reform the
army, Segur (foreign affairs), Mounier, and Chapelier. This
scheme got noised abroad, and was ruined by a decree of
the Assembly of November 7, 1789, that no member of the
Assembly could become a minister ; this decree destroyed
any chance of that necessary harmony between the ministry
and the majority of the representatives of the nation exist-
ing in England, and so at once overthrew Mirabeau's present
hopes and any chance of the permanence of the constitution
then being devised. The queen utterly refused to take
Mirabeau's counsel, and La Marck left Paris. However,
in April 1790 he was suddenly recalled by the Comte de
Mercy- Argenteau, the Au.=itrian ambassador at Paris, and
the queen's most trusted political adviser, and from this
time to Mirabeau's death he became the medium of almost
daily communications between the latter and the queen.
.Mirabeau at first attempted again to make an alliance with
I,afayetto by a letter in which he says, " Les Barnave, les
Duix)rt, les Lameth ne vous fatiguent plas de leur active
inaction ; on singe longtemps I'adresso, non pas la force."
But it was useless to appeal to Lafayette ; he was not a
strong man himself, and did not appreciate " la force " in
others. From the month of May 1790 to his death in
April 1791 Mirabeau remained in close and suspected but
Dot actually proved connexion with the court, and drew
up many admirable ttate-papers for it. In return the court
paid his debts; but it ought' never to be said that he was
bribed, for the gold of the court never made him swerve
from his political principles — never, for instance, made him
a royalist. He regarded himself as a minister, though an
unavowed one, and believed himself worthy of his hire.
Undoubtedly his character vrould have been more admirable
if he had acted without court assistance, but it must be
remembered that his services deserved some reward, and
that by remaining at Paris as a politician he had been
unable to realize his paternal inheritance. Before his in-
fluence on foreign policy is discussed, his behaviour on
several important points must be noticed. On the great
question of the veto he took a practical view, and seeing
that the royal power was already sufficiently weakened,
declared for the king's absolute veto, and against the
compromise of the suspensive veto. He knew from hb
English experiences that such a veto would be hardly ever
used unless the king felt the people were on his side, in
which case it would be a useful check on the representatives
of the people, and also that if it was used unjustifiably
the power of the purse possessed by the representatives
and the very constitutional organization of the people
would, as in England in 1688, bring about a bloodless
revolution, and a change in the person entrusted with the
royal dignity. He saw also that much of the inefficiency
of the Assembly arose from the inexperience of the member.',
and their incurable verbosity ; so, to establish some systeia
of rules, he got his friend Romilly to draw up a detailed
account of the rules and customs of the English House of
Commons, which he translated into French, but which the
Assembly, puffed up by a belief in its own merits, refused
to use. On the great subject of peace and war he supported
the king's authority, and with some success. \Yhat was
the good of an executive which had no power % Let it be
responsible to the representatives of the nation by all
means ; but if the representatives absorbed all executive
power by perpetual interference, there would be six hundred
kings of France instead of one, which would hardly be a
change for the better. Again ilirabeau almost alone of the
Assembly understood the position of the army under a
limited monarchy. Contrary to the theorists, he held that
the soldier ceased to be a citizen when he became a soldier ;
he must submit to be deprived of his liberty to think and
act, and must recognize that a soldier's fust duty is
obedience. With such sentiments, it is no wonder that
he approved of Bouill(''s vigorous conduct at Nancy, which
was the more to his credit as BouiUe was the one hope of
the court influences opposed to him. Lastly, in matters of
finance he showed his wisdom : he attacked NeckerV
" caisse d'escompte," which was to have the whole control
of the taxes, as absorbing the Assembly's power of the
purse ; and he heartily approved of the system of assignats,
but with the important reservation that they should not
be issued to the extent of more than one-half the value of
the lands to be sold. This restriction was not observed,
and it was solely the enormous over-issue of assignats that
caused their great depreciation in value.
Of Mirabeau's attitude with regard to foreign affairs it
is necessary to speak in more detail. He held it to be just
that the French people should conduct their Revolution as
they would, and that no foreign nation had any right to
interfere with them, so long as they kept themselves strictly
to their o\vn affairs. But he knew also that neighbouring
nations looked ^vith imquict eyes on the progi'css of affaira
in France, that they feared the influence of the Revolution
on their owa peoples, and that foreign monarchs were
being prayed by the French emigres to interfere on behalf
of the French monarchy. To prevent this interference, or
rather to give no pretext for it, was his guiding thought as
MlKAiJJbJAU
497
to foreign policv. He Ii^fl teen elected a member of the
comity diplomatique of the Assembly in July 1790, and
became its reporter at once, and in tbis capacity he was
able to prevent the Assembly from doing much harm in
regard to foreign affairs. He had long known Montmorin,
the foreign secretary, and, as matters became more strained
from the complications with ther princes and counts of the
emnire, he entered into daily communication with the
minister, advised him on every point, and, while dictating
his policy, defended it iu the Assembly. Thus in this parti-
colar instance of the foreign office, for the few months
before Mirabeau's death, a harmony was established
between the minister and the Assembly through Mirabeau,
which checked for a time the threatened approach of foreign
intervention, and maintained the honour of France abroad.
Mirabeau's exertions in this respect are not his smallest
title to the name of statesman; and how great a work he
did is best proved by the confusion which ensued in this
department of affairs upon his death.
For indeed in the beginning of 1791 his death was very
near ; and he knew it to be so. The wild excesses of his
youth and their terrible punishment had weakened his
strong constitution, and Ms parliamentary labours com-
pleted the work. So surely did he feel its approach that
some time before the end he sent all his papers over to his
old English friend and schoolfellow Sir Gilbert Elliot, who
kept them under seal until claimed by Mirabeau's executors.
la March his illness was evidently gaining on him, to his
great grief, becau.se he knew how much depended on his
life, and felt that he alone could yet save France from the
distrust of her monarch and the present reforms, and
from the foreign interference, which would assuredly bring
about catastrophes unparalleled in the history of the world.
On his life hung the future course of the Revolution.
Every care that science could afford was given by his
friend and physician, the famous chemist Cabanis, to whose
brochure on his last illness and death the reader may refer.
The people, whose faith iji him revived in spite of all
.suspicions, when they heard that he was on his death-bed,
kept the street in which he lay quiet; but medical care,
the loving solicitude of friends, and the respect of all the
people could not save his life. His vanity appears in its
most gigantic proportions in his last utterances during his
illness; but many of them have something grand in their
sound, as his last reported expression, when he looked upon
the sun — " If he is not God, he is at least His cousin-
german." When he could speak no more he wrote with
a feeble hand the one word " dormir," and on April 2,
1791, he died.
With MirabcKu died, it has been said, the last hope of the mon-
archy; bnt.nirh MarieAutoinette supremeatcourt, canit be said that
there could ever have been any real hope for the monarchy ? Had she
been but less like her imperious mother, Louis would have made a
constitutional monarch, but her will was as strong as Mirabeau's
own, and the Bourbon monarchy had to meet its fate. The subse-
quent events of the Revolution justified Mirabeau's prognostications
in his first memoiie of October 15, 1789. The royal family fled
towards the German frontier, and from that moment there sunk deep
into the heartsof the people not only of Paris, but of the provinces,
a conviction' that the king and queen were traitors to France, which
led inevitably to their execution. The noblesse and the foreign aid
on which the queen relied proved but a source of weakness. The
noblesse, Mirabeau had said, was no army which could fight; and
truly the army of the emigres coiJd do nothing against revolutionary
France iu anus. The inteiTention of foreign aid only sealed the
king's fate, and forwarded the progress of the Revolution, not is a
course of natural development, but to the terrible resource of the
R«ign of Terror. With regard to the Assembly too, and its consti-
tution, Mirabeau had shown his foresight. The constitution of
1781, excellent as it was on paper, and well adapted to an ideal
state, did not deal adequately with the great problems of the time
in France, and by its ridiculous weakening of the executive was
unsirited to a modern state. Surely if events ever proved a man's
vwlitical sagncitv., tb". history of the Ftsnch Sevolutioa proved
.Mirabeau's.
A few words must tc added on Mirabeau's manner of work and
his character.
No man ever so thoroughly used other men's work, and yet
made it all seern his own. " je prends mon bien oil je le trouve "
is as true of him as of Moliisrc. His fir-st literary work, except
the bombaatic but eloquent £ssai sur Ic Despotisnic, was a transla-
tion of Watson's Philip II., accomplished in Holland with the
help of Durival ; his Coi\sidirationa sur Vordre dc Cincinnatus was
based on an American pamphlet, and the notes to it were con-
tributed by Target ; while his financial writings were all suggested
by the Geuevese exile Clavieres. During the Revolutiou he received
yet more help ; men were proud to labour for him, and did not
murmur becairse he absorbed all the credit and, fame. Dumont,
Clavieres, Duroveray, Pellenc, Lamourette, and Reybaz were but a
few of the most distinguished of his collaborator's. Dumont was a
Genevese exile, and an old friend of Romilly's,who willingly prepared
for him those famous addresses which Mirabeau used to make the
Assembly pass by sudden brrrstsof eloquent declamation ; Clavi^es
and Duroveray helped him in finance, and not only worked out his
figirres, but even WTote his financial discourses. Pellenc was his
secretary, and wrote the speeches on the goods of the clergy and the
right of making peace, and even the Abbe Lamourette wrote the
speeches on the civil constitution of the clergy. Reybaz, whose per-
sonaUty has only been revealed within these last ten years, not only
wrote for hira his famous speeches on the assignats, the organization
of the national guard, &c. , which Mirabeau read word for word at the
tribune, but even the posthirmous speech on succession to estates
of intestates, which Tallej-rand read in the Assembly as the last
work of his dead friend. Yet neither the gold of the court nor
another man's conviction woirld make Mirabeau say what he did not
himself believe, or do what he did not himself think right. He
took other men's labour as his due, and impressed their words, of
which he had suggested the underlying ideas, with the stamp of
his olvn individuality; his collaborators themselves did not com-
plain,— they were but too glad to be of help in the great work of
controlling and for^va^ding the French Revolution through its
greatest thirrker and orator. True is that remark of Goethe's
to Ecker-mann, after reading Tlumont's Souvenirs : "At last the
wonderful Mirabeau becomes natural to us, while at the same time
the hero loses nothing of his greatness. Some French journalists
think differently The French look irpon Mu-abeau as their
Hercules, and they are perfectly right. But they forget, that even
the Colossus consists of individual parts, and that the Hercules of
antiqrrity is a collective being^a gigantic personification of deeds
done by himself and by others."
There was something gigantic about all Mirabeau's thoughts and
deeds. The excesses of his youth were beyond all boimds, and
severely were they punished ; his vanity was immense, but never
spoilt his judgment ; his talents were enor-mous, but could yet
make use of those of others. As a statesman his w isdom is indubit-
able, but by no means universally recognized in his own country.
Lovcr-8 of the ancicn rigime abrrse its most forinidable and logical
ipponent ; believers in the Constitrrent Assembly cannot be expected
to care for the most redoubtable adver-sary of their favonrito theorists,
while admirers of the republic of every description agr-ee in calling
him from his connexion with the court the traitor Mirabeau.
As an orator more jrrstice has been done him : his eloquence has
been likened to that of both Bossuet and Vergniaud, but it had
neither the polish of the old 17th-centrrry bishop nor the flashes of
genius of the yourrg Girondin. It was rather parliamentary oratory
in which he excelled, and his tr'ue compeers are rather Burkb anil
Fox than any French speakers. Per-sonaUy he had that which
is the truest mark of nobiUty of mind, a power of attracting love,
and winniirg faithful friends. "I always loved him," ivrites Sir
Gilbert Elliot to his brother Hugh ; and Romilly, wiro was not
given to lavish praise, says, " I have no doubt that in his public
conduct, as in his writings, he was desirous of doing good, that his
ambition was of the noblest kind, and tlrat he proposed to himself
the noblest ends." "What more favourable judgment could be
passed on an ambitiorrs man .' What finer epitaph corrld a states-
man desire !
the best edition of lITraleaii'snOTks is tlint published by Bbncliord in 1S22,
In 10 vols., of TTliicli twiS contain his CZtirres Oratoira; from this collection, liow-
ever, tnany of his less import.int works, and the ilonarthie Pruniennt, in 4 vols.,
17S3, are omitted. For his life consult Mirabeau : Memoiret sur ta vie lilleraire
elprie'.;, 4 vols., 1824, and, what is of most iinporrnnre, Sleimirti iiosrapliijutt,
lilUraires, ft potiliques de Mirabeau ecritspar liii-infme. par ton pere, son oncle, rt
scnfils adoplif, which was issnod by M. Lucas de MonliKiiy in 8vol.<., Paris, 1834.
See also Dumont. Souvenirs sur Mirabeau, 1832 ; Drival. Soucrttirs tur Mtrabeau,
1832 ; victor Hugo, Elude sur Mirabeau, 1834 ; Mirabeau's Jmiendleben. Biolau.
1832 : Schneldcwin, Mirabeau und seine Zeil, Lcipsic, 1831; Mirabeau, a Oje Uis-
tory. London, 1848. The publication of the Correspoudame eiiire Mirabeau el !e
Comie de la Maret, by Ad. Bacoml, 2 vols.. ISOl, marks iin cpcich In onr csact
knowlcdee of .Mirabeau and his career. The most nseful modem books arc Louis
de Lomcnic, Les .Vlrnbeau. 1878, which, however, chiefly treats of lii. father and
uncle: Ph. Plan, Tn Cillaboraleur de Mirabeau. 1S74, trculinB of nc.vbai. and
throwing infinite light on Jlirobean's mode of work ; nini, Instl.v, 11. Rcj-ilalJ,
J/i.vi6f<7ii el la Consliluanle, 1873. On his eloquence and the share his collabora-
tors had in his speeches, seo Atilord, i: MsembUe Couililuanle, 1882 For his
death see the curious brochure of his phjsician Cabanis, Journal iela ^'aladu
:• de la mort de Mirtkeau. Paris, 1791. ("• ''■ '■)
iy8
M I R— M I R
MIBABEAU, VirroE Riqtteti, Maeqois de (1715-
1789), himself a distinguished author and political econo-
mist, but more famous as the father of the great Mirabeau,
was born at Pertuis near the old chateau de Mirabeau on
October 4, 1715. He was brought up very sternly by his
father, and in 1729 joined the army. He took keenly to cam-
paigning, but never rose above the rank of captain, owing
to his being unable to get leave at court to buy a regiment.
In 1737 he came into the family property on his father's
death, and spent some pleasant years till 1743 in literary
companionship with his dear friends Vauvenargues and
Lefrauc de Pompignan, which might have continued had
he not suddenly determined to marry — not for money, but
for landed estates. The lady whose property he fancied was
Marie Genevieve, daughter of a M. de Vassan, a brigadier in
the army, and widow of the Marquis de Saulveboeuf, whom
he married without previously seeing her on April 21, 1743.
[While in garrison at Bordeaux, Mirabeau had made the
acquaintance of Montesquieu, which ufey have made him
turn his thoughts to political speculations ; anyhow it was
while at leisure after retiring from the army that he wrote
his first work, his Testament Politique (1747), which
demanded for the prosperity of France a return of the
French noblesse to their old position in the Middle Ages.
This work, written under the influence of the feudal ideas
impressed upon him by his father, was followed in 1750
by a book on the Utilite des i!tats Provenciaux, full of
really wise considerations for local self-government, which
was published anonymously, and had the honour of being
attributed to Montesquieu himself. In 1756 Mirabeau
made his iirst appearance as a political economist by
the publication of his Ami des Hommes ou traite de
la population. This work has been often attributed to
the influence, and in part even to the pen, of Quesnay, the
founder of the economical school of the physiocrats, but
was really written before the marquis had made the
acquaintance of tiie physician of Madame de Pompadour.
In 1760 he published his TMorie de I'lmjjot, in which he
attacked with all the vehemence of his son the farmers-
general of the taxes, who got him imprisoned for eight
days at Vincennes, and ttcn exiled to his country estate at
Bignon. At Biguon the school of the physiocrats was
really established, and the marquis surrounded himself
with devotees, and eventually in 1765 bought the Journal
de Vagriculture, dv, commerce, et des finances, which became
the organ of the school. He was distinctly recog-
nized as a leader of political thinkers by Prince Leopold
of Tuscany, afterwards emperor, and by Gustavus HI.
of Sweden, who in 1772 sent him the grand cross of
the order of Vasa. But the period of his happy literary
life was over ; and his name was to be mixed up in
a long scandalous lawsuit. Naturally his marriage
had not been happy ; he had separated from his wife
by mutual consent in 1762, and had, h& believed,
secui'ed her safely in the provinces by a lettro de cachet,
when in 1772 she suddenly appeared in Paris, and soon
after commenced proceedings for a -separation. The poor
marquis did not know what to do ; his sons were a great
trouble to him, and it was one of his own daughters who
had encouraged his wife to take this step. Yet he was
determined to keep the case quiet if possible for the sake of
Madame de Pailly, a Swiss lady whom he had loved since
1756. But' his wife would not let him rest ; her plea was
rejected in 1777, but slie renewed her suit, and, though
the great Mirabeau had pleaded his father's case, was suc-
cessful in 1781, when a decree of separation was pro-
nounced. This trial had quite broken the health of the
marquis, as .well as his fortune ; he sold hia estate at
Bignon, and hired a house at Argenteuil, where he lived
auietly till his death on July 11, 1789.
For the whole family of Mirabeau, the one book to refer to i*
Louis dc Lomenie's Les Mirabeau, 2 vols., 1878, and it is greadyto
be regretted that the talented author did not live to treat the live*
of the great Mirabeau and hia brother. See also Lucas de Mon-
tigny's Miriwires dc Mirabeau, and, for the marquis's economical
views, Ds Ja Vergne's Ecoiiomistcs frati^is dv. 18** siicU.
MIKAGE. See Light, vol. xiv. p. 600.
JUEAMON, Miguel, a Mexican soldier of French
extraction, was born in the city of Mexico, September 29,
1832, and shot along with the emperor Maximilian ac
Queretaro, June 19, 1867. While still a student he helped
to defend the miUtary academy at Chapultepec against the
forces of the United States; and, entering the army in 1852,
he rapidly came to the front during the civil wars that dis-
turbed the country. It was largely due to Miramoa's support
of the ecclesiastical party against Alvarez and Comoiifort
that Zuloagawas raised to the presidency; and in 1859 he
was called to succeed him in that office. Decisively beaten,
however, by the Liberals, he fled the country in 1860, and
spent soma time in Em-ope earnestly advocating foreign
intervention in Mexican affairs ; and when he returned it
was as a partisan of Maximilian. His ability as a soldier
was best shown by his double defence of Puebla in 1856.
MIRANDA, Francesco (1754-1816), was born at
Santa F6 in New Granada in 1754. He entered the army,
and served against the English in the American War of
Independence. The success of that war inspired him
with a hope of being the Washington of his own countiy,
and a belief that the independence of Spanish America
would increase its material prosperity. With these views
he began to scheme a revolution, but his schemes were dis-
covered and he had only just time to escape to the United
States. Thence he went to England, where he was intro-
duced to Pitt, but chiefly lived with the leading members
of the opposition — Fox, Sheridan, and Romilly. Finding
no help in his revolutionary schemes, he travelled over the
greater part of Europe, notably through Aiistria and
Turkey, till he arrived at the court of Russia, where
he was warmly received, but from which he was dismissed,
though with rich presents, at the demand of the Spanish
ambassador, backed up by the envoy of France. The news
of the dispute between England and Spain about Nootka
Sound in 1790 recalled him to England, where he saw
a good deal of Pitt, who had determined to make use
of him to " insurge " the Spanish colonies, but the peaceful
arrangement of the dispute again destroyed his hopes. In
April 1792 he went to Paris, with introductions to Potion
and the leading Girondists, hoping that men who were work-
ing so hard for their own freedom might help his countrj--
men in South America. France had too much to do in
fighting for its own freedom to help others ; but Miranda's
friends sent him to the front ^vith the rank of general
of brigade. He distinguished himself under Dumourioz,
was intrusted in February 1793 with the conduct of the
siege of Maestricht, and commanded the left Tving of the
French army at the disastrous battle of Neerwinden.
Although he had given notice of Dumouriez's projected
treachery, he was jjut on his trial for treason ou May 12.
He -was unanimously acquitted, but was soon again thrown
into prison, and not released till after the 9th Thermidor.
Ho again mingled in politics, and was sentenced to be
deported after the struggle of Vendiimiaire. Yet he escaped,
and continued in Paris til) the coup d'etat of Fructidoi
caused him finally to take refuge in England. He now
found Pitt and Dundas once more ready to listen to him,
and the latter sent a special minute to Colonel Picton,
the governor of Trinidad, to assist General Miranda's
schemes in every possible way : but, as neither of fhcni
would or could give him substantial help, he went to the
United States, where President Adams gave him fair words
but notliing more. O^ice more he returned to England,
\
M 1 K — M I K
499
where Addington might have done aomething for him but
for the signature of the peace of Amiens in 18D2. At the
peace, though in no way amnestied, he returned to Paris,
but was promptly expelled by the First Consul, Who was
then eager to be on good terms with the court of Spain.
Disappointed in further efforts to get assistance from
England and the United States, he decided to make an
attempt on his own responsibility and at his own expense.
Aided by two American citizens. Colonel Smith and Mr
Ogden, he equipped a small ship, the "Leander," in 1806,
and with the help of the English admiral Sir A. Cochrane
made a landing near Cardcas, and proclaimed the Colombian
republic. He had some success, and would have had more
haid not a false report of peace between France and
England caused the English admiral to withdraw his
support. At last in 1810 came his opportunity; the
events in Spain which brought about the Peninsular
War had divided the authorities in Spanish America, some
of whom declared for Joseph Bonaparte, others for
Ferdinand ML, while others again held to Charles IV.
At this moment Miranda again landed, and had no difficulty
in getting a large party together who declared a republic
both in Venezuela and New Granada or Colombia. But
Miranda's desire that all the South American colonies should
rise, and a federal republic be formed, awoke the selfish-
ness and pride of individual provincial administrations,
and thus weakened the cause, which further was believed to
be hateful to heaven owing to a great earthquake on
March 26, 1812. The count of Monte Verde, the Bourbon
governor, had little difficulty in defeating the dispirited
forces of Miranda, and on July 26 the general capitulated
on condition that he should be deported to the United
States. The condition was not observed; Miranda was
moved from dungeon to dungeon, and died in 1816 at Cadiz.
There are allusions to Miranda's early life in nearly all memoirs of
the time, but they arc not generally very accvirate. For his trial see
Buchez et Roui, His'.oire ParUmentairc, xivii. 26-70. For his
later life see Biggs, History of Miranda's Attempt in South America,
London, IS09 ; and Yeggasi, JUvolueion de la Columbia.
MIRANDOLA. See Pico.
MIRKHOND (1433-U98). Mohammed bin Khiwand-
sh&h bin Slahmiid, commonly called Mlrkhwind or ^Ilrk-
hAwand, more familiar to Europeans under the name of
Mirkhond, was born in 1433, the son of a very pious and
learned man who, although belonging to an old Bokhara
family of Sayyids or direct descendants of the Prophet,
lived and died in Balkh. From his early youth he applied
himself to historical studies and literature in general. In
Herit, where he spent the greater part of his life, he gained
the favour of that famous patron of letters, Mlr'Allshlr
(born 1440), who served his old school-fellow the reigning
sultan Husain (who as the last of the Tlmiirides in Persia
ascended the throne of HerAt in 1468), first as keeper
of the seal, afterwards as governor of Jvujin. At the
request cf this distinguished statesman and writer'
Mirkhond began about 1474, in the quiet convent of
KhilAsIyah, which his patron had founded in Her4t as a
house of retreat for literary men of merit, his great work on
universal history, the largest ever written in Persian, and
to the present day an inexhaustible mine of information
both to Eastern and Western scholars. It is named
Rauzat-ussafd fi sirat-vlanbid walmuluk waWmlafd or
Garden of Purity on the Biography of Prophets, Kings, and
Caliphs. That the author has made no attempt at a critical
examination of historical traditions can scarcely be called a
^>eculiar fault of his, since .almost all Oriental writers are
equally deficient in sound criticism ; more censurable is his
' Mir 'Alishir not only excelled as poet both in Cbaghatai, in
which bis epopees gained him the foremost rank among the classic
■.vritere in that language, and in Persian, but composed an excellent
tadhkirah or biography of contemnorary Persian poets.
flowery and often bombastic style, but in spite of this draw-
back, and although, in our own age, the discovery of older
works on Asiatic history has diminished to some extent
the value of Mirkhond's Rauzat, it stQl maintains its high
position as one of the most marvellous achievements in
literature from the pen of one man, and often elucidates, by
valuable text-corrections, various readings, and important
additions, those sources which have lately come to light.
It comprises seven large volumes and a geographical ap-
pendix ; but internal evidence proves beyond doubt that the
seventh volume, the history of the sultan Husain (1438-
1505), together vrith a short account of some later events
down to 1523, cannot have been written by Mirkhond
himself, who died in 1498. He may have compiled the
preface, but the main portion of this volume is probably
the work of his grandson, the equally renowned historian
KliwAndamlr (1475-1534), to whom also a part of the
appendix must be ascribed.
The following is a summary of the contents of the other six
volumes. Vol. i. : Preface on the usefulness of historical stndies,
history of the creation, the patriarchs, prophets, ar.i rulers of Israel
down to Christ, and the Persian kings from the'mythical times of
the Pesbdadians to the Arab conquest and the death of the last
SisanianYazdajirdlll.inSO A.H. (651 A.D.). Vol. ii.: Mohammed,
Abiibekr, 'Omar, 'Othman, and *Ali. Vol. iii. : The twelve imams
and the Omayj'ad and ' Abbasid caliphs down to 656 a.h. (1258 A.D.).
VoL iv. : The minor dynasties contemporary with and subsequent to
tiie 'Abbasids, down td 778 a.h. (1376 a.d.), the, date of the over-
tlirow of the Kurds by Timur. Vol. v. : The MoglnJs down to Timiir's
time. VoL vi. : Timur and his successors down to Sultan Hnsain's
accession in 873 A.H. (1468 A.D.). The best accounts of Mirkhond's
life are De Sacy's "Notice sur Mirkhond" in his Mimoires sur
diverses antiquity de la Perse, Paris, 1793 ; Jourdain's "Notice de
I'histoixe universelle de Mirkhond" in the ^iotices et Extraits, vol.
ix., Paris, 1812 (togetherwith a translation of the preface, the history
of the Ismailiaus, the conclusion of the sixth volume, and a portion
of the appendix) ; Elliot, History of India, vol. iv. p. 127 sq. ;
Morley, Descriptive Catalogue, London, 1854, p. 30 sq. ; Rieu, Cat.
of Persian MSS. of the Brit. Mus., vol. i., London, 1879, p. 87 sq.
Mirkhond's patron, Mir 'Alishir, to whom the Rau^t is dedicated,
died three years after him (1501)^
Besides the lithographed editions of the wholewoik in folio, Bombay, 1S53, and
■Teheran,^ 1852-56, and a Turkish Tersion, Constantinople, 1S42, tlie following
portions of Mirkhond's histoo" have been poblished by European Orientalists :
Early Kings of Pcrtia, by D. Shea, London, 1832 (Oriental Translation Fund);
L'Siitoire de ta djffiaslie des Satsanidcs, by S. de Sacy (in tJie above-mentioned
Memoirei) ; Bittoirt dcs Sattanides {ttxte Penan), by Jaubert, Paris, 1843 ; Hit.
toriapriorum regvm Persarum, Pers. and Lat., by Jenisii, Vienna, 1762; Mirehondi
ItisCoria Taheridat-um. Pevs. and Lat., by Mitscherlik, Giittingen, 1814, 2d ed.,
Berlin, 1819 ; Eistcria Samanidarum, Pers. and Lat., by Wilken, Gottlngen.
180S ; NisCoire dee Samanides, translated by Defr^mery, Paris, 1845; Bistorta
OAarneriAw'um, Pers.'and Lat., by Wilken, Berlin, 1832; Getchiehteder Syltaneaua
dem OescfiieeJtte Bi^eh, Pers. and German, by Wiiken, Berlin, 1835; followed by
Ertlmann's Erldutervng vttd Ergdntvng, Kazan, 1836 ; Bistoria Seldichuekidarwn,
ed. Vullers, Giessen, 1837, and a Gc.man translation by the same: Biitoire des
Sultans du Eharesny in Persian, by Defr^mery, Paris, 1842; Bislonf of iJle
Alabeks of Syria and Persia, in Persian, by W, Morley, London, 1848; Bistori/s
OAuridarum, Pers. and Lat., by Mitseherlik, Frankfort, 181S; Sistoiredes SuUans
Chuvides, translated into French by Defr^mery, P-trSs, 1844; Vie de Djenghii-Khan,
in Persian, by Jaubert, Paris, 1S41 (see also extracts from the same fith volume
in French tj-anslation by Langlfes in vol. vi. of Notices et Extraits, Paris, 1799,
p. 192 sq., and by Hammer in Sur les origin^ Pusses, St Petersburg, 1825, p.
52 s;.}; "Tfmilr's Expedition against Tuktamish Khdn," Persian and French,
by Charmoy, in il^moires de I'Acad. lmp&. de St Petersbourg, 1836, pp. 270-321
and 441-471. (H. E.^
MIEOPOLIE, a town of Russia, situated in the govern-
ment of Kursk, district of Suja, 83 miles south-west of
Kursk and 25 miles from the Sumy railway station. It
is supposed to have been founded in the 17th century,
when it was fortified against the raids of Tartars. The
fertility of the soil led to the settlement of large villages
close by the fort, and the 10,800 inhabitants of this town
are still engaged mostly in agriculture. There is also an
extensive manufacture of boots.
MIRROR. It is only since the early part of the 1 6th
century that mirrors have become articles of household
furniture and decoration. Previous to that time — from the
12th to the end of the 15th century — pocket mirrors or
small hand mirrors carried at the girdle were indispensable
adjuncts to ladies' toilets. The pocket mirrors consisted
of small circular plaques of polished metal fixed in a shallow
circulir box, covered with a lid. Mirror cases were chiefly
madft CrJ ivory, carved with relief representations of lov.~
500
MIRROR
or domestic scenes, hunting, and gs^es, and sometiniei-
illustrations of popular poetry or romarice. Gold and
silver, enamels, ebony, and other costly materials were
likewise used for mirror cases, on which were lavished the
highest decorative efforts o£ art workmanship and costly
jewelling. The mirrors worn at the girdle had no cover,
but were furnished with a short handle. In 625 Pope
Boniface IV. sent Queen Ethelberga of Northumbria a
present of a silver mirror; and there is ample evidence
that in early Anglo-Saxon times mirrors were welLknown
in England. It is a remarkable fact that on many of the
sculptured stones of Scotland, belonging probably to the
7th, 8th, or 9th century, representations of mirrors, mirror
eases, and combs occur.
The method of backing glass with thin sheets of metal
for mirrors was well known in the Middle Ages at a time
when steel and silver mirrors were almost exclusively
employed. Vincent de Beauvais, writing about 1250, says
that the mirror of glass and lead is the best of all " quia
vitrum propter transparentiam melius recipit radios." It
is known that small convex mirrors were commonly made
in southern Germany before the beginning of the 16th
century, and these continued to be in demand under the
name of bull's-eyes (OclisenrAugen) till comparatively
modern times. They were made by blowing small globes
of glass into which while stiU hot was passed through
the pipe a mixture of tin, antimony, and resin or tar.
When the globe was entirely coated with the metallic com-
pound and cooled it was cut into convex lenses, which of
course formed small but well-defined images. It appears
that attention was drawn to this method of making mirrors
in Venice as early as 1317, in which year a "Magister de
Alemania," who knew how to work glass for mirrors, broke
an agreement he had made to instruct three Venetians,
leaving in their hands a large quantity of mixed alum and
soot for which they could find no use.
It was, however, in Venice that the making of glass
mirrors on a commercial scale was first developed; and
that enterprising republic enjoyed a rich and much-prized
monopoly of the manufacture for about a century and a
half. In 1507 two inhabitants of Murano, representing
that they possessed the secret of making perfect mirrors
of glass, a knowledge hitherto confined to one German glass-
house, obtained an exclusive privilege of manufacturing
mirrors for a period of twenty years. In 1564 the mirror-
makers of Venice, who enjoyed peculiar privileges, formed
themselves into a corporation. The products of the
Murano glass-houses quickly supplanted the mirrors of
polished metal, and a large and lucrative trade in Venetian
glass mirrors sprang up. They were made from blown
cylinders of glass which were sUt, flattened on a stone,
carefully polished, the edges frequently bevelled, and the
backs "silvered" by an amalgam. The glass was remarkably
pure and uniform, the " silvering " bright, and the sheets
sometimes of considerable dimensions. Li the inventoi-y
of his effects made on the death of the great French
viiinister Colbert is enumerated a Venetian mirror 46 by
25 inches, in a silver frame, valued at 8016 Uvres, while
a. oicture by Raphael is put down at 3000 livres.
The manufacture of glass mirrors, with the aid of Italian
workmen, was practised in England by Sir Robert Mansel
early in the 17th century, and about 1670 the duke of
Buckingham was concerned in a glass-work at Lambeth
where flint glass was made for looking-glasses. These old
EngUsh mirrors, with bevelled edges in the Venetian
fashion, are still well known.
The Venetians guarded with the utmost jealousy the
secrets of their varied manufactures, and gave most excep-
tional privileges to those engaged in such industries. By
their statutes any glassmaker carrying his art into a
foreign state was ordered to return on the pain of
imprisonment .of his nearest rela;tives, and should he
disobey the command emissaries were delegated to slay
the contumacious subject. In face of such a statute
Colbert attempted in 1664, through the French ambassador
in Venice, to get Venetian artists transported to France to
develop the two great industries of mirror-making and
point-lace working. The ambassador, the bishop of
Biziers, pointed out that to attempt to send the required
artists was to court the risk of being thrown into the
Adriatic, and he further showed that Venice was selling to
France mirrors to the value of 100,000 crowns and lace to
three or four times that value. Notwithstanding these
circumstances, however, twenty Venetian glass-mirror
makers were sent to France in 1655, and the manufacture
wav'begun under the fostering care of Colbert in the
Faubourg St Antoine, Paris. But previous to this the art
of blowing glass for mirrors had been actually practised at
Tour-la- ViUe, near Cherbourg, by Richard Lucas, Sieur de
Nehou, in 1653; and by the subsequent combination of
skill of both establishments French mirrors soon excelled
in quality those of Venice. The art received a new impulse
in France on the introduction of the making of plate glass,
which was discovered in 1691. The St Gobain Glass
Company at[i Ibute the discovery to Louis Lucas of Nehou,
and over th ioor of the chapel of St Gobain they have
placed an inscription in memory of " Louis Lucas qui in-
venta in 1691 le methode de couler les glaces et installa la
manufactm'e en 1695 dans le chateau de Saint Grobain."
Manufacture. — The term "silvering," as applied to the forma-
tion of a metallic coating on glass for giving it the properties of &
mirror, was till quite recentlj a misnomer, seeing that till ahout
1840 no silver was used in the process. Now, however, a large
proportion of mirrors are made by depositing on the glass a coating
of pure silver, and the old amalgamation process is comparatively
little used.
The process of amalgamation consists in appljTng a thin amalgam
of tin and mercury to the surface of glass, which is done on a
perfectly flat and horizontal slab of stone bedded in a heavy, iron-
bound wooden frame, with a gutter running round the outer edge.
On the surface of this table, which must be perfectly smooth and
level, is spread a sheet of thin tin-foil, somewhat larger than the glass
to be operated on, and after all folds and creases have been conj-
pletely removed, by means of stroking and beating with a covered
wooden rubber, the process of " quickening '* the foil is commenced.
A small quantity of mercury is rubbed lightly and quickly over the
whole surface, and the scum of dust, impure tin, and mercury is
taken oiF. Mercury is then poured upon the quickened foil, until
there is a body of it sufficient to float the glass to be silvered (about
\ inch deep), and, the edge at one of the sides having been cleared
of the scum peculiar to mercury, tho glass (scrupulously cleaned
simultaneously with the above operations) is slid from that side over
the surface of tho mercury. Weights are placed over the surfaeo
until the greater part of the amalgamated mercury is pressed out,
the table is then tilted diagonally, by means of dumb-screws, and
all superfluous mercury finds its way to the gutter. The glass
is loft twenty-fom' hours under weights; it is then turned over
silvered side up, and removed to a drainer with inclining shelves,
whore by slow degrees, as it dries and hardens, it is brought to a
vertical position, which in tho case of largo sheets may not be
arrived at in less than a month. This process yields excellent
results, producing a brilliant silver-white metallic lustre which is
only subject to alteration by exposure to high temperatures, or by
contact with damp surfaces ; hut the mercurial vapours to which
the workmen are exposed give rise to the most distressing and fatal
aflbctions.
In 1835 Baron Liebig observed that, on heating aldehyde with
an ammoniacal solution of nitrate of silver, in a glass vessel, a
brilliant deposit of metallic silver was formed on the surface of the
glass. To this observation is due the modern process of silvering
glass. In practice tho process was introduced about 1840 ; and it
IS noT carried on, with several modifications, in two distinct ways,
called the hot and the cold process respectively. In tho former
method there is employed a horizontal double-bottomed metallic
table, which is heated with steam to from 35° ia 40° C._ The glaM
to bo silvered is cleaned thoroughly with wet whiting, then washed
with distilled water, and prepared for the silver with a sensitizing
solution of tin, wliich is well rinsed off immediately before its
romov.al to the silvering table. The table being raised to the
proper temperature, the glass is laid, and the silvering solution a*
I K R O R
^^^r.??. f f^" > '"'?'? ""^ '"=*' ^f ">« t^W^ has time to dry
any part of the snrfajje of the glass, the solution used is prepared
nitrate of Sliver are dissolved; to thU there U added of liquid
^^nT/'?-!^- <'S80)?2mmmea; the mixture is mtered, and
^^!i"P , ^j^'^t^ "■'"' <^*'^«'i ™ter, and r 5 grammes of tartaric
About?"? Tf^ "" ^° ^"^"^ "^ ^*'^' "» mixel^ith the solntio™
to be s^vi d ^'l^r'^A "•"" ^h'- «'f^ f" "''<='' ^"P"ficial metre
to be sJver^d The metal immediately begins to deposit on the
glass, which IS maintained at about 40° 0(104° F. ), and i^ little
rf«n/° Y^ r '■°"/ -continuous coating of silver iT formed
The silvered surface is then cleaned by very ^utionsly wipineTith
a very so t chamois rubber, and tr^ted^a second ^tZ^tl a
acid, ibis solution is applied m two portions, and thereafter the
l^H°/™ """^ '^'"^^^^ '^'^""^ of ^ nna'ttached sUvS and
refose and removed to a side room for backing up
in sUvenng by the cold process advantage is taken of the nower
of mverted sugar to reduce the nitrate of silver. This proceS^hS
^otobtv^f^fT"" '!'^»"«ri^g?f■^irrors for astrononil^'teles»i^t^
notably for Leverner's great telescope in the Paris Observatory for
oA„* '• *". °«'^'''- ,Two solutions are prepared, the first of which
tte^W ''t k""'.^'' ^-"^ ^' »^~°'* t^=^"g»^ prepStion. For
of n' teto of1°mf^- ^"^T- °^'^*y*" "^ '^^" »'"i 1200 gimmes
1 1^^? of ammonium are dissolved in 10 litres of water, and 13
SrKniP'?7-^"?''°i.?^? ^ '" "t^ "f '^^t^f. "ad of each of these
Bolntions 1 litre is added to 8 litres of water, which is aUowed t^
SmiVf """" ''?^°" ^"'l '''™ decanted The seconTsolS^
o?£3S-F"^ -^^^^^^
• Lf i operated on 15 cubic centimetres of the silver solution
above d^cribed ar« measured out, and from 7 to 10 per cent o^'
tt^lT^T "^ "T'-'^.d ™gar is added, both being nuickl?sti^edto
^if^i^'^iP'T''' '^P''"y ^°d evenly over the gll^. The rXction
"iok&Wart-^l'- -'"«™^^ibits lints pa^i^gThrough
toSspSand tbf^ '^. ""/tout seven minutes it again becomes
^ exTemelv thin nnS°"i "' ""l?' '^ <">'^V^^^- Thi? first deposit
Th7^T^!\ A ; ■ *"•"" *<> transmission of bluish ravs
^n.lf^T^'^ '?'""°" '^"^ ""^"IS aid unattached dust-lfk;
SSh ii^tin/n '» " 'T^'^^y '^P^d <"^ ">« ^"^-■■ed surface washed
e^tentXlf Aer° t'l^'" V^^'.f ^^'' *^ "'^■^^d ^olutions^to the
^rf„.= ! • '"/quantity used in the first application. The finished
fS^l .VP*'^ """^ ^'^^^''^d in the most tLrough manner -for
fi,rtw *^°" "' '^"^^''= ''"'* '^ft would destioy the Sw The
«bS^nnH?r »^ -'n""" °" ?'^' '= °°t 5° adherent and unalter-
?h tinmercS^ 'Ir^' of sunlight and sulphurous fiimes as
Xl,,i '^Z^ amalgam, and moreover real silvered glass has a
wluch instantaneously forming a kind of amalgam render th?deno?it
nrot^c? Z fv'"'" fl,'^ "^r fi"nlyadhe^nt than before To
S^mL . \- ■" "^tallio film from mechanical injury and the
tZ^^ *°"°°v. "^ eases and vapours, it is coated^A sheUac
to Jfnire^tfr;^:;-!",^-^ IIZI whSyTtC If f '^
adherent deposit of platinum is formed "on the Sai rsoInHon 7f
Srin,Tors ntd '^''P'^T'' 'T' «™amentailetters, i-c.
In Oriental c^nw;?^"'"",?' "=**' ^''^ ^"" '" common use
tinue to b„Tf ■ ?°d especially in Japan and China they con-
thamSst remS^ period men?L „f ^^'"k''?'''^ ^"? ""'"^ f'™
literature of the K^S^^'Ve 'eoutedTI 'f»''^^ Chinese
minor nreserved at Ui iJ^' Z- ("^eputed) first made Japanese
Japan and a^ancieni 1,^ ° "''■'''=' "^""^ ^'S^"'* veneration in
* the'effect that i wL^' \TJ'"''='* "'* "^'^^ is a tradition
■f tte emptre L a SS" ^^- '^ ^u-VSoddess at the foundation
mimL or^L^ Pnnapal article of the Japanese regalia. The
." tTtMks fr ^3 ri""' r-.''"'Tn general they con!
metal ^ritt haS/rst' n^ne p^t" nc'riif' °''^^^fT
.».n.r is slightly convex in forai,''rtiiat':':eS ?d"J^^ °'set
501
proportionately reduced in size; the back of the disk is occnnied
Zm,'^r:iT^lT''r "^^^^tation andt^scripS^I^
h^lLen at^ted^ tb. ° -'''^ ^ *^ ^"^^^ M"<=h attention
u^oeen attracted to these mirrors by a singular nhvsical necnli
attracted 'atSnhT''^"^ "Y"'^ ^J *^ JapanesTb^ut S^ ClLl?
aciractea attention as earlv as thp n+Ti ro«+,,L. ^ ^^u-xna »t,
possessed of this property^S among* the ?Sse at "STo"
even twenty bmes tie price sought for the ordi^ non-semWve
examp es The true explanation of the mr^iu?™ ^ w
fefl'^-''^ the Frencfi physicist Persou,Tho Xrv^ SI
the reflecting surface of the mirrors was not mufo™j7conye"
the portions opposite reUef surfaces being pla^^ Se'
A^lr^ ^','^^-'' "J^' "^y' '■^fl^'c'^ fr"" tfe convex poSon
rtlf ^"^ ^Z^ •"" * ^^^^y iUuminated imageT whSe on
the contrary, the rays reflected from the planTrSrtioL of* the
mirror preserve their paraUelism, and appear on l,e screen L an
S^^t^ofT^S-t *C«=nt^ast with t^^e feeblerlmSati^n o°
sSrfl^ aie is'^n l-?\* r^ ^""'''' °f Pl«°^ "^ the mi?ro
tS -t^ an accidental circumstance due to the manner in
Pe^ L ir'""^' V'f''., '==Tiained by Professors Ayrton an^
rtrry, by whom ample details of the history, process of maS.
facture, and composifion of Oriental mirrors ?ave beeTpubSd.
fhf ct?'dfs7 °f ^"°°i? P°!i=l"-ng the surface consistsTsr^
no^Ho^, l^t y -"^ direction with a sharp tool. The thicS
of the tooUhan t" ."v '« 'f ' "^f' ""1 '■^^'^^u'c^ '0 tie pressure
at fi„t = the thm flat portions, which tend to yield aiidfonn
rL= ff ^^^T" ^Yl^"'' ''"' ">'^ ^y the reaction of its elaaS
nVW ItT"''^!-^'"* ^"""^ * ^"^'•"y """''^ surface while ?S?more
[a? if Portwns are comparatively Uttle affected. This irregu-
^v^ of ^ffac? -^ inconspicuous in ordinary light, and do^ f^t
visibly distort images ; but when the mirror reflate a bright liZ
on a screen the unequal radiation renders the minute dSen<^ of
surface obvious. The ingenious theory of Person hasTen^b-
rf ^riW^i^i^^'sfiTfi?'' "r "'"''*'"' ,''y "• «»" to t''^ acXi,
Rprthf^n^ nt^' ^^ ■"?" '"^""y ^y investigations of MM
ser vof x.?^ ^^- ®'' ^'"^'" * ^^^ '' ^Phy^u^ (5th
' ^^'- (J. PA.)
Ancient Mirrors.
atMn <^ f I «la=sieal antiquity („iT.TT,o,, apeculum) was
osUaUv^rL-lS"°tt 'Y"?, """"^ ™ ""^ »'de and poUshed,
Tf^Irf. t 'r'* ,* 'i?°'"'' ^o-netimes momited on a stand
in the form of a female figure (see Costuihe, vol. vi p. 463
fig. 1), sometimes fixed inside a circular bronze case. The
common si^e is that of an ordinary hand mirror. Examples
large enough to take in the whole figure appear to have C!
w; b„i fT f.i^^^ '=■"■' ■u^utioned, and tfiSngh none of them
sin.^1,0^^'"^ f'\' '^'^''"'=" ""'^ "■" 1^ questioned altogether,
smce the process of silvering occasionaUy employed on bronze Siirrori
B,f th^v "r """'"Sr P^-^^^^ -"^y ''''''= been applieTto^C
show, thlt ^ '°' """lu" °^ '°,''™" ="" ^^^'"S from antiS
shows that bronze was the regular material employed. The lllov
known as speculum, producing a very hard metal with great reflecting
fZJ^ K "'"'Pa-f "vely seldom met with. SUver mirrors are m^-
tioned, but none have as yet been found.
yZ^f^J™"}?^^ J^^^^^.ol. ^Y-'^nt mirrors. especiaUy those of
vm. p 648). While twelve incised specimens are all that are
h/n2r"" fr' ^r""-.'^' °"""^' ''"""d in Etriii^a m^l
t,V.w,^ a thousand. As a nilo the subjects incised are
S^o JT ^"^i^A ^yf-^'ogy and legend, the names of th^
^T^alt^T^'V""'^ '"^''''"]^ ^^''^'' '° l^'™'<^n letters
and orthography. In most cases the stj'le of drawing, the types
?i ''i^/?u'^-'. an.a lie manner of composing the groups are to^e
tJ^A /'"aractenstics of Greek art. Some may havJ been Z!
morel r^f^-f,!^,; l^V' the greater number appear to have been
more or less faithfully imitated from such designs as occurred on
llt^^l"'°T"^°^^ r"^'^ ^'-^^l' vases wfich the Etr^ns
,°n^ f ^ J"" ^v""- . ^T"" ''here distinctly Etruscan figures are
mtioduced such as the heroes ^lius and CceUus Vibenna on a
niirror in the British Museum. Greek models are followed. The
characteristics of Greek art here referred to date fi-om a little before
400 B.O., and last for some time after. In this period would fall
the majority of the Etruscan mirrors, and to this period also belone
tbe Ureek incised mirrors, among which may be mentioned for the5
Beauty one representing Leucas and Corinthus, inscribed with their
names (engraved, Monununis Grecs, 1873, pi. 3, published by the
Association pour 1 encouragement des Etudes Grecques), and another
m the British Museum (Oazitle Arch., ii pi. 27), on the back of
which IS a figure of Eros which has been silvered over. With this
last-mentioned mirror was found the bronze case used to contain it,
502
M I R— M I S
on tho back of which is a group of AphrocHto and Eros in rcpoussie.
It was found in Crete. But most of^the Greek mirrors and mirror-
cases having artistic designs are from Corinth. One I'sars the name
of tho artist, 'AttowSs inolei (engrarcd. Arch. Zciiung, 1862, pi.
166, fig. 1).
Archaic art (about 500 B.O.) is represented by a mirror in the
British Museum from Sunium in Attica. The mirror itself is quite
plain, but the stand is composed of a draped female figure, above
whose head float two cupids. From Etruria there is a comparatively
small number :vith archaic incised designs. It maybe concluded that
the luxury of mirrors enriched with incised designs was not freely in-
dulged^ before 400 B.C. iu Etruria and never to any extent in Greece.
A special centre of incised mirrors was the Latian town of Prsneste
^Palestrina), and it is of interest in regard to some of the mirrors
found there that'they have inscriptions in early Latin. Artistically
they have a purely Greek character. Plain mirrors are found
wherever Greek and Roman civilization spread, and it may be seen
from a specimen found in Cornwall, now in the British Museum,
that the Celtic population of England had adopted the form and
substance of the mirror from their conquerors. This specimen is
enriched with a Celtic pattern incised. The shape of the handle
testiiies to native originality. Mirrors were used in Greece, perhaps
rarely, for divination, as appears, for example, from Pausanias (vii.
21, 5), the method being to let tho mirror down into a well by
means of a strin" till it reached close to the surface of the water.
\V'hen it was puUed up after a little it was expected to show the
face of the sick person on whose behalf the ceremony was performed.
This was at Patras. .
Tho principal publicotions on ancient mirrors ovo Gcrhnrd, EtruskUche SpifgeL
Bdlin, 184S-C7, 4 vois., containing 430 plates; for the Gicek minors, Mylonaa,
'EAATjvtKci icaTOJiTpa, Athens, 1876, and Dumont, Bullet, de Corresp. Selle'it., 1877,
p. 108 ; see also Friederichs, Kleinere Kmst und Indusl>-ie tin Atterthumy Diissel-
uorf, 1871, p. 18 sq.; and Marquardt and Mommsen, Handbuch del- romisrhcn
AlltrlhuiTM; rii.pt. 2, p. C70. (A. S. M.)
MfEZAPUR, a district in the North- Western Provinces
of India, lying between 23° 51' 30" and 25° 31' N. lat.,
and between 82° 9' 15" and 83° 0' 36" E. long., is bounded
on tbe N. by Jaunpur and Benares, on the E. by Shah4bdd
and LohirdagA, on the S. by SargiljA state, and on the W.
by AUahibAd and Rewah state, and has an area of 5217
square miles. It is crossed from east to west by the
Vindhya and Kilimur ranges. A central jungly plateau
connects these, and separates the valley of the Ganges
from that of the Son.
The population in 1S72 was 1,015,203 (males, 520,496; females,
494,707), of whom 049,644 were Hindus, 64,809 Mohammedans,
and 750 Christians. The non-Asiatic population numbered 623.
Only three towns had a population exceeding 6000 : — Mirzapur,
67,274; Chanar, 10,154; and Ahraura, 9091. Out of a Govern-
ment-a.s3essed area of 3048 square miles, 1313 are cultivated, 497
cultivable waste, and 1233 uncultivabie. The part of Mirzapur
which lies north of the Vindhyas is very highly cultivated and
thickly peopled, but the rest of the district consists largely of
ravines and forests, with a very sparse population. Local manu-
factures comprise carpets of a superior desciiption, brass ware, and
shellac. The East Indian Railway traverses the district, along the
right bank of the Gauges, tor a distance of 32 miles. "Tlie climate
is slightly warmer and damiier than that of districts farther north
and east. The mean annual rainfall is 42'7 inches.
MirzApur, chief town and administrative headquarters
of the above district, is situated on the south bank
nf the Ganges, 5G miles below AllahdbAd (25° 9' 43" N.
lat., 82° 38' 10" E. long.). The population in 1872 was
67,274, of whom 55,917 were Hindus and 11,053 Mo-
hammedans. Up to quite recent years MirzA])ur was
the largest mart in upper India for grain and cotton ; but
of late its commercial importance has rapidly decreased,
owing to the establishment of through railway communica-
tion with Bombay via Jabalpur, and the rise of Cawnpore
to the position of a mercantile centre. Tho river front,
lined mth stone fjhdts or flights of stairs, and exhibiting
numerous mosques, Hindu temples, and dweUing-houseis of
the wealthier merchants, with highly decorated facjad^s and
lichly carved balconies and door-frames, is handsome ; but
the interior of the town is mainly composed of mud lint?.
rhe manufacture of shellac gives cmiiloyment to about four
thousand persons ; brass ware and carpct-s are also made.
rhe imjJorts consist of grain, sugar, cloth, metals, fruit,
apices, tobacco, lac, salt, and cotton ; tin; same articles,
ivitli manufactured lac-dve. shellac, and qhi, are escorted.
MISDEMEA3T0UK. " The word misdemeanour," says
Russell {Oil Crimes, voL i. chap, iv.), " is applied to all those
crimes and offences for which the law has not provided a
particular name." Stephen, in his Digest of ike Criminal
Law, adopts the following mode of distinguishing between
misdemeanour and other crimes. " Every crime is either
treason, felony, or misdemeauoui'. Every crime which
amounts to trea.son or felony is so denominated in the defini-
tions of crimes hereinafter contained. All crimes not so
denominated are misdemeanours." _It is customary to speak
of misdemeanour as implying a less degree of crime than
felony (see Felony). " ilisdemeanours," observes Russell
in the passage already cited, " have been sometimes termed
misprisions ; indeed the word misprision, in its larger sense,
is used to signify every considerable misdemeanour which
has'not a certain name given to it iu the law, and it is said
that a misprision is contained in every felony whatsoever,
so that the offender may be prosecuted for misprision at the
option of the crown." Misprision, in a more restricted sense
(or negative misprision), is the concealment of an offence.
Positive misprisions are contempts or misdemeanours of a
public character, e.g., mal-administration of high officials,
contempt of the sovereign or magistrates, A'C. The rule
as to punishment, when no express provision has been made
bylaw, is that "every person convicted of a misdemeanour
is liable to fine and imprisonment without hard labour
(both or either), and to be put under recognizances to keep
the peace and be of good beha-\-iour at the discretion of
the court" (Stephen's Digest, art. 22). By 28 & 29 Vict,
c. 67 prisoners convicted of misdemeanour and sentenced
to hard labour shall be divided into two di\'isions, one of
which shall be called the first division, and when a person
convicted of misdemeanour is sentenced to imprisonment
without hard labour the court may order him to be treated
as a first-class misdemeanant, who shall not ba deemed
a "criminal prisoner" within the meaning of that Act.
The Prison Act, 1877 (§§ 40, 41), requires prisoners con-
victed of sedition or seditious libel, or attached for contempt
of court, to be treated as misdemeanants of the first class.
In New York and some other States of the American
Union the legislature has defined felony as any crime
which is or may be punishable with death or imprisonment
in a State prison, all other crimes being misdemeanours.
MISHNAH. The Mishnah, in the most familiar appli-
cation of the name, is the great collection of legal decisions
by the ancient rabbis which forms in each Tabiud the text
on which the Gemara rests, and so is the fundamental
document of__the oral law of the Jews. The question
What is Mishnah? was asked, however, as early as the
latter part of the 1st or the early part of the 2d century,
though in a somewhat different sense and for a somewhat
different purpose.^ It will be answered in the course of
this article in all its bearings.
1. Name. — Rabbinic tradition has fixed the pointing
Mishnah (HJP'D) by giving its status- eon^ruclus as
Mishnath. Although the word Mishnah is not found in
the Bible, it is no doubt a classical Hebrew term, signi-
fying something closely akin to Mishneh (which term
occurs more than once there), as may be seen on comparing
Mikvah with Mikvch, Miknqh with Mihieh, Ma'alak with
Ma'aleh, and Mar'ah with Mar'eh, each two of which are,
however they may vary in practical application, un-
questionably synonymous terms. Tho practical signifi-
cations of Mishnah are seven in number : — (1) repeti-
tion, i.e., tradition :- as such it is the equivalent of the
' See T. B., A'irfrfi«Ain,.49(i.
' The root Shanok (Hiw'), from which ilishnah is immediately de-
rived, is not merely, as is often thought, to Uam, to Uach, byt to
royeat : and it is in reaUty this last nieaaicg which naderhes tho twu
lors.n.
I S H N A H
503
ZcvTcpaxTW of Epiphanius,^ the tradkiones et trurepuKrai
of Jerome,' the hemipac-vi of Justiaian,' and the n*3iJ'
mirft (" ^^^ second to the law ") of the Aru/ch* ; (2) re-
citation from memory, in contradistinction to reading from
a book ;5 (3) study : as such it Li the equivalent of
Midrash, in the former part of its third signification ; (4)
instruction : as such it is the equivalent of Midraah in
the latter part of its third signification ;° (5) system,
style, view, line of study and instruction : as such it is
identical with .the Talmudical ShittaA;'' (6) a paragraph
of the Mishiah: it is invariably employed in this sense in
the Babylonian Talmud, and is identical with the word
Salakha/i, used for the same purpose, in the Palestinian
Talmud; and (7) the collection of the decisions of the
whole " oral law," i.e., the Mishnah in the concrete sense.
The word- Mishnah has three difierent plurals : — (1) the
traditional Muhnayotk for signification (7), formed on
the analogy of Mikvaoih (not, as some think, on that of
Mikraotk or Midrathoth) ; (2) the correct, though ques-
tioned, Minhniyyoth for signification (6), formed on the
analogy of Panhiyyoth from Paro^hak (or Parshah), not
to speak of that of Maadyyoih from Ma'oie/i ; (3), the
somewhat irielegant, but correct, -MisknotJi,* which also
serves for signification (6). Significations (1), (2), (3),
(4), and (5) have, however inconsistent it may appear
when one takes into consideration their respective equi-
valents, no plural whatever. So much for the Hebrew
Mishnah. The Aramaic Slathnitho will be spoken of
later.
2. Contents and Nature. — The Muhnah consists chiefly
of Halakhah;^ there is, comparatively speaking, little
Agadah i" to be found in it. It is not, however, as many
think, either a commentary on the Halakhic portions of the
Pentateuch, or on the ordinances of the Sopherim, or on
both together. It rather presupposes the knowledge of,
and respect for, both the Mosaic and the Sopheric laws,
and it only discusses, and finaUy decides on, the best mode
and manner of executing these. The discussions and
eventual decisions to be found in the ifishnah owe their
existence principally to deep meditation on these two
kinds of laws, notably on the former, by the rabbis of
various ages, but chiefly by those who lived fifty years
before and one hundred and fifty years after the rise of
Christianity, the names of whom it faithfully gives, along
with their respective discussions and decisions. There are
but few cases to be found in the Mishnah which would
critically come under the denomination of an Halakhah U-
Mosheli mis-Sinai, i.e., an explanation (of a law) as directly
* Userts., XV. («oTck ypafifiareuv), in fine. Epiphanios was a native
of Palestine, even if he was not, as some think, of Jewish parentage.
A3 a Palestiniaa writer on Jewish and senrii.Jewish matters he must
have had a more than superficial knowledge of the Jewish traditions
(the Mishnah, &c. ). And indeed, to judge from the account he gives
of the various Jemsh traditions (although the text of this account is
extremely corrupt in every way), he was pretty well informed. For
he tells us tliat the Jews have four kiuds of traditions : — such as are
ascribed to Moses (by which he no doubt means the Halakhah le-
Mosheh mis-Sinai) \ such as are ascribed to the sons of Asmcna^us
(by which he means the Telfanoth, &c., of the Beth Dim shel Hash-
riionai; see T. 'B.,'Abodah Zarah, 366); such as are ascribed 'to E.
'Akibah (the great teacher and martjT) ; and such as are ascribed to
R. Andan, &c. (Rabbi Ychudah Hannasi).
- In Jsaiam, cap. viii. 11-15.
' A'ov. cxlvi. (nsfpl 'EBpaluv) Ki*. i, tn medio.
* Article nJCD (first defiuil-oa).
' Contrast Shanoh (DJE') with Kan (KljJ).
^ • See article JIidrash, p. 285.
'See Schlller-S'inessy, Catalogue of Hebrew ilSS. in the ..amoridge
University Library, ii. p. 94.
a See MS. Add. ■404 (Univereity Library, Cambridge), leaf 283J.
" This word, derived from the root Halokh (i?n), to go, is synony-
mous with Minhag (custom, practice) and Mishjiai (rule), &c
^'^ For the meaning of this term and the Agadic parts which are to
be found in the Mishnah. se^ Mttjeass.
given by God to Moses, and in uninterrupted sucoesblon
received from him by the rabbis. Several cases given
under this name in the Mishnah are not bona fide cases ;"
for the test of such an Halakhah is that it must never
have been contested by any one.>^
3. Method. — ^A Mishnah, if genuine, never begins wth
a passage of the Pentateuch, and even comparatively
seldom brings direct proof from or gives reference to it.
When there is any exception to this rule it will be found,
on close examination, either that such a paragraph belongs
to a very early age (that of the Sophenm), or that it is to
be found in another work of the " oral law," and is simply
copied in the Mishnah, or, what is more likely, that if
independent, it belongs to a very late age, or, finally, that
the proof or the reference thus given is only a later addi-
tion. One example of the true method of the Mishnah will,'
perhaps, better illustrate the foregoing statement than a
sheet full of theorizing on the subject; and this one ex»:mple
will the more surely suffice because of its mixed (Mosaic
and Sopheric) character. It is the very first paragraph of
the whole Mishnah, and runs thus : "From what time (of
the day) does (may, should) one read the Shema' ('the
taking upon oneself the yoke of the heavenly kingdom ')
in the evening 1 " The Mishnah does not begin : One is
in duty bound to read the Shemd in the evening, because
it is written (Deut. vi. 7), " And when thou liest down."
For, in the first place, the law to read the Shemd evening
and morning is not unquestionably Mosaic, as the words,
"And thou shalt talk of them, &c.," do not refer to
this passage of the law particularly, but rather to the
words of the Pentateuch in general;" and, secondly, it is
needless to say that one is in duty bound to recite the
Shemd twice a day, since every Jew readily acknowledges
this duty and executes it, although it is not Mosaic. This
duty of reading the Shemd, the grounds on which this
duty rests, and how it is best fulfilled, are fully and
ably discussed, developed, and finally settled in that
part of the Talmud called Gemara,'^* — the business of
which it is to discuss the words of the Mishnah and to
show the sources of the tradition, and eventually the pas
sage in the Pentateuch (if on such the case rest) from
which the respective disputants had derived their views, etc.
4. Pwryjosf.— Although it is a book containing Halakhic
decisions, the Mishnah was never intended, as many think,
to enable the reader thereof to decide from it immediately.
This mistake is old '^ and widely spread, — but a mistake
nevertheless. The purpose of the Mishnah was and h
simply to exhibit the development of the "oral law"
and the view taken of this development by the rabbis of
various times. For this reason one finds side by side
with the opinions of the majority those also of the
minority, which latter are very carefully given. But
why, since these opinions of the minority can have no
decisional effect ? The Mishnah itself ('Eduyyoth,^^ i. 5)
"■ See R. Asher b. Yeliiel (Harosh), Hitekhoth Mikvaoih (coming
close after tins R.abbi's commentary on Niddah, in the printed editions
of the Bab. Talmud), i. 1.
" There are, however, at least sixteen such bona fide Cases to be found
in the works of the "oral law."
" See T. B., Berakhcth, on Deut. xi. 19.
" Oetnara, or Gernoro, siguifies concretely discussion on and final
settlement of the contents of the Mishnah, from ge'.:mr (ICIi), to study
deeply, to come to a final result ; which last signification is, to some
extent, to be found also in the Hebrew root gamor (103). Compare
T. B,, Boho Metsi'o, 33a, and Kashi, in loco.
" Sc3 T. B., Sota!i, 22a.
" The word niny is variously pointed:— '^dayott, 'Ediyoth, and, as
in the text, 'Edvyyoth, whicli last, if the name come from {WIS,
because of the testimony of the witnesses on which this Massekhelk
chiefly rests, would be the only correct one. But it ought to be
remarked that the Babylonian teachers must have spelled it 'Idi'rjoth
(best things), since its eqniv.-ilent is given by them as Lihirij (or
Behirotho). See T. B., Berakhoth, 27a and elsewhere.
504
M i h M jN A il
answers this question : it is that the teacher or the judge
of later ages may he thus enabled, if he have good grounds
for taking a view different from that of the majority as
given hundreds of years before, to reverse the old decision,
liy forming, on the strength of the example before him,
with others who agree with him (or without them, if
only one vote was wanted to reverse the majority) a fresh
majority. Thus the Jewish " oral law " can never become
ossified like the laws of the Medes and Persians.
5. Language. — The Mishnah is, on the vhole, written
in almost pure Hebrew ; and even the originally non-
Hebrew words (Aramaic, Greek, Latin, itc.) are so skil-
fully Hebraized that they are a most creditable testimony
to the linguistic powers both of many of the disputants
mentioned in it, whose very words are in most cases given,
and of the editor ' or editors who revised them.
6. Age and Authorship. — R. Yehudah Hannasi (the
Prince), the reputed author (in reality only the principal
and best among the editors) of the Mishnah, was born
before the year 140 of the Christian era. His name was
in full Yehudah b. Shime'on b. Gamliel b. Shime'on b.
Gamliel- b. Shime'on b. Hillel. On account of his holy
living he was surnamed Eabbenu Hakkadosh, and on
account of his great learning and authority he was called
simply "Rabbi" ("My Teacher" ^xire^cfWfiice). Rabbi and
his lime, however, are no tenninus a quo for the composi-
tion of the Mishnah. For, not' to speak of many isolated
Mishniyyoth which can be brought home to R. Meir, to R.
'Akibah, to Hillel,' to Yose b. Yo'ezer,* and to others, even
to the earliei- Sopherimf we find that R. Yose b. Halaphta
of the 1st century already quotes the beginning and end-
ing of a whole Mishnic treatise (Kelim''), and that in the
same century (or very early in the 2d) another treatise
consisting of early testimonies ('Eduyyoih '') was put into
order. Moreover, although the phrases Mishnath Ji.
Eliezer h. Ya'akob^ and Mishnath E. 'AMbah^ do simply
signify the systems, styles, and views of these two
eminent teachers, there can be little doubt that they and
others besides them, presided over colleges in which the
whole Halakhic matter was systematically treated and
regularly gone through. Nor are Rabbi and his time for
the composition of the Mishnah a terminus ad quevi, for the
Mishnah was not brought to a close till a very long time
afterwards. Not only did R. Hiyya Rabbali, R. Hosha'yah
Rabbah, and Shime'on bar Kappara redact Mishnayoth,^"
but in the Mishnah before us notices are actually found
Avhich reach to the end of the 3d century, if not even later.
The statement that Rabbi was the first to ViTite down the
^ The Hebrew si)oken in the house of the principal editor of the
X^ishnah was so coirect that rabbis actually learnt the meaning of
uncommon words of the Bible from the handmaidens of this house.
See T. B., Hash Hasshanah, 266. As for Kabbi himself, he was not
merely a fine Hebrew scholar, but a fine Greek scholar also. He was
nlso a purist ; for in T. B. , Sotah, 494, he is reported to have exclaimed,
" Why should any one speak in Palestine ' Sursi' ! Let him speak
cither Hebrew or Greek ! " In using the word " Sursi " for " Surith "
(Syi-iac), he no doubt makes a punning allusion to the mixed (cut-up)
iharacter of the language, corrupted from Hebrew, Chaldee, Persian,
Greek, and Latin.
- This was the teacher of St Paul. ■
* In atldition to such well-known Agadic.^/'iVAntyyoM as those whicn
;Te distinctly ascribed in Aboth to Hillel, see Mishnah Kiddushin, iv.
I ; and contrast it with the language and stylo of the Mishnah in
general, and that of Massckhto Kiddushin in particular.
* Mishnah' EdiLyiioUt, viii. 4.
* See Mishnah Ma'astr Shcni, v. 7; Sotah, v. 1, 2; l^ega'im, xii.
5, 6, 7, &c. ; though it cannot bo said that these passages preserve
tlic teaching of the So2)ho-im in their original purity.
'' SQe'Mishnah Kdim, in fine.
' SceT. 'B.,Bcrakhoth, 2Sn : " It is handed down orally (Njn) that
J!d:iyyDlh w.ts on that day (when R. El'azar b. 'Aiao'ah was installed
AS presi'lcnt) gone through," i.e., redacted.
«T. 13., I'ebamolh, 49b.
* Mishnnh Sjfnhcdrin, iii. 4.
" See ^(ihckik Ralluh on ii. 8 in medio.
Mishnah is untrue, because the thing is impossible. ' For
the two Talmuds, of which that of Babylonia was not
finished before the 6th century (if then), know, certainly,
nothing of the writing down of the Mishnah. On the
contrary, their language throughout presupposes ihe Mish-
nah in their time to have been what its name indicates, a
repetition, i.e., a thing acquired by continual recitation,
because, like the other works of the " oral law " {Torah
shclbe'al peh), it was to be, and Vfas, handed down orally.'^
As for the difficulty of keeping in memory such a stu-
pendous and vast work as the Mishnah, it is sometimes
forgotten in this controversy that memory was aided by
a great variety of mnemotechnic means, such as numbers
and names of teachers, and by the existence of other works
of the " oral law," which, although they also were not
written down, could be easily kept in memory because
they rested on letters, words, and verses of the written
Pentateuch. Anyhow, there is ample evidence, both nega-
tive and positive, that the Mishnah as we now have it
was not committed to writing in the times of Rabbi or
for long afterwards. But it certainly does not follov
that no merit is due to Rabbi in connexion with the
Mishnah. His merit in connexion with it is great in
every way. For (1) Rabbi was himself a link in the
chain of tradition, since he had " received " from his
own father and so on up to his ancestor Hillel and even
higher ; (2) he gave in the Mishnah his own decisions,
in most cases in accordance with those of the famous E.
Mcir, which are thus in a great part secured to us ; (3)
in giving his own decisions he preserved to us also a
good many decisions of the teachers of the 2d century ;
(4) in collecting all these decisions he anxiously ascertained
the genuine formulas of the older Mishniyyoth ;'- (5) he
did not merely reproduce the formulas which he esteemed
the best, but discussed them anew in his own .college,
which was composed of men of the highest eminence, as
is well known; (6) although he gave on the whole the
very language of the teachers who preceded him, he
gauged it, guarding it against the barbarisms which are
so plentiful in the other works of the " oral law " ; and (7)
he scattered the Mishnah broadcast (though only by word
of mouth) over all Palestine and Babylonia by means of
the disciples who flocked to him from all parts of those
countries. K the Mishnah, as it now exists, is not entirely
his, it certainly belongs to him in a great measure and in
more than one sense.
7. Value and Appreciation. — Whatever can be said in
favour of the Agadah applies with equal if not greater
force to the Mishnah, as the litter is a canonical and
therefore more reliable work of the "oral law." The
Mishnah is one of the richest mines of archaeology which
the world possesses. But it waits yet for the master
touch to break the spell which holds it bound. Great,
however, as the value of the Mishnah is, its popu-
larity has never been steady, but has been continually
fluctuating, and that for various reasons. Even Rabbi
in his time had to ai>peal for due attention to it. Whilst
it was neglected in troublous times by the masses, who
ran after the Agada/i,^^ which, besides being consoling,
needed no particular study, it was, in prosperous times,
neglected by the rabbis themselves through the study of
the Bible and the Talmud." And much more was this
" See particiJarly T. B., JSobo SIclsCo, 33a and, ft; and compare
also Rashi, in hco. , ■ ,
'- See T. y., Ma'aser SItcni, v. 1; and compare the' preceding note.
" See MiDRASH, p. 285, note 14.
" R. Yohanan said, This Mishnah {Doraitho), that no study can cx^
eel that of Gemara, was taught in the time of (and by) Rabbi himself.
Thou the people went after Gemara and neglected the study of the Mish-
nah. Whereupon ho ajnin bade them ever nin more after Mishnah
than iifttr Criiinjv. T. B., B'Jio Mctsi'o, ZZb, and Rashi, in. loco.
M I S H N A H
505
thi case when the Talmud had developed, from a mere
gtndious activity to two concrete works of large size.
8. The Ultimate Writing Doim of the Mishnah. — The
troubles of the unhappy Jews had multiplied everywhere.
The masses, as already stated, preferred, in consequence of
these troubles, the Agadah. But the number of the
learned also diminished through these troubles day by day ;
and the comparatively few that remained preferred more
and more the Talmud (in Palestine the Palestinian and in
Babylonia the Babylonian), which was a better field for
the exercise of their ingenuity. The fate of the Mishnah
would' have been sealed had it not been ultimately
written down. But the writing down of Halakhah en
masse had been prohibited in early times. Two considera-
tions, however, ultimately removed all scruples. (1) It
was a time to do something for God, even if by such doings
BQs law was apparently destroyed.' Le^ne (and a minor)
law be disregarded, so that many (and higher) laws be
preserved. The Halahhoth of the Mishnah were numerous
and the studeiits few ; the power of tyranny increased and
that of the memory decreased by reason of the persecution.
(2) The language of the Mishnah, although pure, and in-
deed purer than the language of several books of the Bible,
was so concise and terse that it could not be understood
without a commentary; and, therefore, even after being
written down, it would virtually retain its oral character.
9. Recensio7is. — The Mishnah has three principal recen-
sions : — (1) the Mishnah as presented in the work standing
by itself ; (2) that on which the Palestinian Talmud rests ;
and (3) that of the Babylonian Talmud. The first-named
and the kst-named Mishnayoth have always been known
as complete ; the second, however, was supposed for
several hundred years to be imperfect, lacking four
Pei-akim in Shahhath, two entire Massehhioth in the Seder
Nenkin, the whole of the Seder Kodoshim, and by far the
greater part of the Seder Tohoroih.- But since 1869 this
recension also has been kno^\'n to have been always com-
plete ; and it is to be found in its entirety in a MS. pui^
chased in that year for the University Library of Cam-
bridge (Add. 470. 1). Besides these three there are many
minor recensions, touching, however, only isolated read-
ings. These last are to be attributed chiefly to copyists.
The origin of the difference between the principal recen-
sions is to be sought in the following two facts : — (1)
Rabbi had himself gone twice through the Mishnah and
had himself considerably altered the wording of the text;'
and (2) his successors in early and late times had wilfully
altered and corrected the original text.
10. Dimsions and Detailed Contents of tlie Uishnah. — Tbe ilish-
nnh in all recensions is divided into six Scdarim (ordere), each of
which contains a number of Massck-htoth* (treatises), which stand
in connexion with one another. These are subdivided into Pera^im
(chapters), and these again into Halnhhoth or Miskniyyoth (para-
graphs called Mishnoth).' The number of the Scdarim is six,
that of the MassclcMoth sixty,' and that of the Pcrakim 523, or,
* This is a somewhat inexact application of Ps. cxix. 126, but it has
licen more than once acted upon both in ancient and modem times by
the Jews. Compare the explanation given in T. B., BcraUtoth^ 63a,
and Menahoth, 99a.
* Xiddalt is the only ifasselheth of this Setter of which three entire
Perakim are to bo fonnd in the printed editions. Compare Schiller-
Szinessy, Occasional Kotlces, kc, i. (Cambridge, 1878, 8vo) p. 8.
' See T. B., Bobo JitctsCo, Ua, and elsewhere.
* Whether the word ilassekheth comes from Masokh CnDD, to pour
into, to mix, &c.), or from Nasokh (^bO, to pour, to mix, to weave,
tc), it signifies in cither case here a mould, a form, a frame. Mas-
tekhelh has three several plurals :— (1) the common MasseklUoth (not
*Uassikhloth) ; (2) the less common Massekhoih (see MS. Add. 470. 1,
belonging to the University Library of Cambridge, leaf 69a and else-
where) ; and (3) Massekhtiyyoih (nVnaDD), see Midrash Rahbah on
Canticles \i. 8, 9. The Aramaic MasseklUo (not ilassikhto) has in the
plur.ll ilassekhotho, the use of which is. however, very uucommou.
' Compare above, p. 503.
* Compare Midrash Rahbah on CanticlM \\. 8, 9.
10—10*
with a fourth Pereji: to BUckurim, 624.' The following Is z schema
of the whole Zfishnah.^
I. Zera'im (on Agriculture, preceded by the Treatise on Thanks-
givings'). (1) Bcrakhoth lyAessiags), in nine chapters ; (2) Pcah
(Lev. six. 9, &c.), in eight chapters; (3) Demai (fruit, grain,
&c., doubtful if tithed), in seven chapters ; (4) Kil'ayim (mixtures
of plants, animals, and garments respectively), in nine chapters ;
(5) SheWUhi^eux of release), in ten chapters ; (6) Tcriimoth (gifts
to the priests), in eleven chapters ; (7) ila'aser Sheni" (Deut. xiv.
22-27), in five chapters ; (8) Ma'aser Rishon, otherwise Ma'ascroth
(I^evitical tithes), in five chapters ; (9) HallaJi (Num. xv. 19-21),
in four chapters; (10) 'Orlah (Lev. xix. 23), in three chapters;
and (11) Bikknrim (Deut. xxvi. 1-10), ia thiee (commonly four)
chapters.
II. Mo'ed (on Festival Times). (1) Sliablalh (Sabbsth), in
twenty -four chapters; (2) 'Enibin (mixtures, i.e., ideal union of
divided spaces), in ten chapters ; (3) Pesah (commonly Pcsahim,
i.e., Passover), in ten chapters ; (4) Kippurim (commonly Ymna,
i.e., " the day " [of atonement]), in eight chapters ; (5) Shckalim
(Exod. XXX. 12-15), in eight chaptei-s ; (6) Sukkah (Lev. xxiii.
34-43), in five chapters ; (7) Bdsah ("an egg," so called from the
beginning of the treatise; also Yom Tob, i.e., on work prohibited,
or permitted, on festivals), in five chapters ; (8) Rash Ilasshanah
(on the various kinds of new year, as religious or civil, the king's
accession and coronation, &c.), in four chapters ; (9) Tdaniyyoth
(fast-days), in four chapters ; (10) Mcgitlah (reading of the book of
Esther, other readings, &c. ), in four chapters; (11) Hagigah
(festival-offerings), in three chapters; (12) ilashkin (so called from
the be^nning of the treatise, but commonly Mocd Katan, on work
prohibited, or permitted, on the middle holidays of Passover and
Tabernacles), in three chapters.
III. Nashim (Women). (1) Nashim (so called from the first
distinctive word of the treatise, but commonly Yebamoth, on
sisters-in-law, the le\'irate, kc), in sixteen chapters; (2) EctMiloth
(marriage-pacts, settlements, kc), in thii-teen chapters; (3) Ncdari^n
(vows), in eleven chapters; (4) Nazir (Num. vi, 2-21), in nine
chapters ; (5) Qittin (bills of divorcement and other bills), in nine
chapters; (6) Kiddushin (beti'othal and marriage), in four chapters;
(7) Sola (mostly Sotah, Num. v. 12-31), in nine chapters.
IV. Nezikim, commonly J\'<;ji7.-iK (Damages, &c.; see E.xod. xxi. ,
xxii., kQ.). (1) 'Kczikin (commonly Bobo Kammo, the Former
Gate, in ten chaptere ; Bobo Mctsi'o, the Sliddle Gate, in ten
chapters; and Bobo Baihro, the Last Gate, in ten chaptere"), in
thirty chapters; (2) Syixhedrin (courts of justice, &c.), in eleven
chapters; (3) iCakkoth ("forty stripes save one," &c.), in threo
chapters ; (4) Shcbuoth (oaths, &c. ), in eight chapters ; (5) 'Eduyyoth
(testimonies) or 'Idiyyoth (chiefest or best things '-), in eight chap-
ters ; (6) 'Ahodtth Zarah (idolatry), in five chapters; (7) yiboth'
(see MiDRAsn, p. 286), in five chanters ; (8) Uorayoth. (judicial]
errors, teachings, and decisions), in three chapters.
V. KoDOsniM (Holy Things). (1) Zebahim^' (sacrifices), in.''
fourteen chapters ; (2) MenaJtoth (meat-oflerings), in thirteen!
chapters ; (3) ShehiUith Hidlin (slaying animals for common food;
commonly ITullin, or common food), in twelve chapters ; (4) Bc'i
khoroth (the first-boi-n of beast and man), in nine chapters ; (6)j
'Arakhim, commonly Urachin (on valuations ; seo Lev. xxvii.j
2-33), in nine chapters ; (6) Tcmwah (Lev. ix. 10, 33), in seven'
chapters ; (7) KaretMh, not Kerithoth (sins the punishment of whicK|
is excision), in six chapters; (8) Mc'ilah (Num. v. 6, 7), in six chap-
ters; (9) Uiddolh (description of the temple and its measurements ;
see Midrash, p. 286), in five chapters ; (10) Tamid (perpetual or
daily sacrifice), in sLx (commonly arranged in seven) chapters ; (11)
Kinnim (sacrifices of birds), in three chapters.
VI. ToHOROTH (Purifications). (1 ) A'f/i'm (impurities of vessels),
in thirty chapters ; (2) Oholoth (Num. xix. 14-16, &c.), in eighteen
chapters ; (3) Ncya im (plague of leprosy in man, house, and
j garment), in fourteen chaptere; (4) Parah (Num. xix. 1-19), in
twelve chapters ; (5) Tohoroth (euphemism for impurities), in ten'
chapters ; (6) Mikvaoth (religious baths), in ten chaptere ; (7)
Niddah (Lev. xv. 19-33), in ten chapters ; (8) Maklishirim (liquids
' Othere include, instead of a fourtli Perek of Bikkmnm, the Perek
Rabbi Meir, i.e., the treatise " On the Acquisition of the Law." The
original Mishnah, however, had neither of these two Perakim.
' In this scheme the Cambridge JIS. of the Mishnah is taken as
the groundwork, while the variations in title, &c., are given from the
common texts.
' Corap.ire St Paul's words, Eph. v. 20, tSxapiiTToiJiTej irdj'TOTr
inrep trivTiav.
'" Oa the apparent anomaly of Ma'aser Sheni preceding Ma'astr
Rishon, see Schiller-Szinessy's Catalogue of Hebrew MSS. m tiu:
Cambridge University Library, vol, ii. p. 1, note 4.
» In the Cambridge JIS. Add. 470. 1, Massekhto Setikln is given
correctly .is one, containing thirty chapters. Compare T. B. , B<Ao
Kammo, leaf 102a, 'Abodah Zarah, 7a, and Midrash Shemuel, v.
n See p. 503, note 16.
u Also known under Shehitath J^odoshim.
506
piedi^iposing for the contraction of imparities, Lev. -i 34) in sii
U. EdUio,is.-TU editions of tho Jfishnah, wlietlier as a book
by Itself or as contained in the Babylonian Talmud are too
numerous to be mentioned here. The JLp^.^cm li the
m^Zv^ Tt V.T'^'" \''?h ^"'"-^'^'^ (withMai^nonM s's com
P 50l) afdTt^t ''^"^'"'?. °"'"™"y '^ i-'complet'e tZSe
Psee Iri;,-! W « • ■ "'°^T'"' ™f"'^'"'l by the scribe of 1288-89
(see Schiller-Szinessy, Occasiomt Polices, &c., i. pp. 8 11) The
7^iTl °/w- ^'"r'-'="J- P!-'^^= of Cambridge have tVere o^c aid the
leaine.1 public nnder considerable obligations by publishing for the
first time the complete original i)/M»aA on which the Pa?esan an
U^^r''' ''"^ "^-^ ""'1- MS. preserved in th^ Um'Sy
^ 12. Translations —There exist translations of the Mishnah in
the ln'oHferA''b'"f ^°flf'^ .(" T'^'re is a Latin Lnstt ^n b^
the In others Abendana (R. Ya'akob and R. Yitshak) Th/f„rm„
'almottSTuT^^ufartT.eVti""'™'-^" °" *^ ^^"''""^ "-
^1^ enumerated here tL^ ' ?' f" ?^r°',*"^f°'-'= ^e sped-
%f-&,i.-^„^^th£^t -
jviz., tnatonro/ioroM) has appeared in the collection
MISHNAH
,.. , .^'"^ ^\-.'?- Lowe's able edition of this erand wml- in..
MMomokuh the Palestinian Tahnud r\2. Sri.ll'SiJ':
lers""^™ p'sirR' vft^lT'^r "{^^'Olo-Jcoish nutary, London,
n»:^TSL^ni^iy"£?ii'^^r|:^td
WagensoU (SoteA), Cocceius (;l/""foW) Fairs ?^;Lif t"'"','^
Talmud will one day come to light somowhcreTn he E^t see Sch ler
fcniessy in the Acadany, February 23, 1878 /^.-cwi ,7- ,'
^olc^ Udasi Yedc Ocmim, kc. (Berlin, 1856, 8vo). (3) The com
mentary on vanoua treatises of the B. Talmud and iridltflfi
ra!sr(?;^.zrri.r^r«^^ret^^^
H=«s°^?s-ngi^i-iSS r
centuries. His commentary ou tlio tI Sud and th!l in^^ ". ''
on the Mishnah. h now beinc- published S. the vl,^-"^"'^
Babylonian Talmud.' (5) Th°e cCmentary of ElhiTAsit ' U
those parts of the B. Talmud on which that " nriJ,™ '.f ^ '
tators- wrote. Here ought to ba meitioned^^o the Tpa";:?:
editwprinccps of tliis commentary as far as the^i<,*«!s ?f
cerned, which appeared at Leghorn in ?653-54 8vo m Th:
supplements and ad.litions to life commentary of Eashibv hi It
m-kw Rabbenu Ychudah b. Nathan (c.^.Tt. B l^alLft^ fof
Ras'hbr^'^ ^^ ^t S"""^^""^ I^''^™" Shemuel 'b 1 eM^
^m&t^t>^1.,r»U^^^~£3
and opponent of Maimonides) on the orde?. J'zcrfinv (w^h sS^
ments taken from the works of the somewhat older KYitSb
S^ l"^''^',??'^ r^/«™«A.= (10) The commentary by K. Met o'
.mler fl3^\ W ''mf^f ""?"" of Rudolph of ^Ha^sburg), see
maer (13) below. (11) The commentary by R Asher b YeW
(a disciple of the foregoing, who died at Toledo in 1 4n n„ ' tJ ■»
one treatises of the orders i and vi hAtk! ^32/) on twenty-
n ,L H ii°",'f "'"/ ™ *''* "h"!'^ ^/mAmA, by R. Yomt?b L?^'
mann Heller (flourished in 16th and l/th centuries? TbirforT^r
(Pi^'u- -fi'-.^omeof the greatest cong"Sns IfV^lZ
meSyofR'"ZroTRo«rr'' ^^^Poralel much of Ihe com-
14 L°;,f; o , o Kothenburg ; compare under (10).
ostensibly the Aramaic equivalnt of tlffneW;. if!fnWu,hxyM,^
\t^''}T'-"- *i -=-^- tdMpriset n r STev'er^'
I'll' W^^A^x^sirt t/x; ,^:l^€ F^
law, and many literary notices of Mklm.V 7ni Xf • t '""^ °™'
teachers from time immemorial, notably R. 'Akibah Ind R
poiaS in t svjf "'r^K^" °f ^bis additio'nal matt! nSor"^
E^hII , T'^"^ ""^ ""^ '^■'"lonical i/wA.mA. is called Toscvhah
n lamaV'VW" <""■ ^^^^'f" ^' '"""^ '"^^ correctly ,^iiO
already ?i the Talt^^T"" f^^f' T^ 't "'''^"' P'"™' "ecu
?>,„ j7 ; 1 /." "'.""fs and Mtdrashnn," Tosephlo shans with
the A^,s;„„A, which it enlarges and explains, the number of order^
and treatises, but not that of chapter^, of vVhich it ° as only 45^
Tie odest collection of Tosepht ic matter even a^ fll M^^:;
collection of Mishuic matter, is' du% to R. •Akiteh. But, wlfilsl
, « In the synod called together by Rabbenu Gershora, amon- several
onetir"' ° °""' "'*' "'' ^'^ '' '^'°^"'' to "'"■n- more tS!
J ^il'T'^ff"^ !"'-^^.'^""' ''I'P«»«<» »t Paris in 1868, and that
ou MakMth at Leipsic in 1876, both in Svo
Rabbe''uTYvl"l ^'"^tl'"'' ""\R»bbeuu Meir another son-in-law and
Rabbenu Yaakob another grandson of Rashi) are tho Hrst of the ac-
the urn ::si::^.' ^""^^ ""^-"^ ^-""-" "o™ '' ^h' ea^; "rcr
tol^w'"'-''.';. » \T,f ?'?''>' "^ ^'""'<' Printed under his name.
172o, 4to), is really his is still matter of dispute
?™fw \^'y^""'' ^««A O" Ecclesiastcs v. 8, &c. There can he Uttlo
M I S H N A H
507
tiic Mishnah, as a work, waa first sifted by his disciple K. Meir,
Tostplito, as a work, was first sifted by another disciple E. Ncheray ah ;
and just as E. Meir's Mishnah was sifted again by Sabii and others
after him, and was not writtcu down before the 6th century, so
Tosephto was sifted again by K. Hiyya, K. Hosha'yah, and others,
and was not written down in its' entirety before the 6th century.
It is no wonder, then, that it now contains matter of a considerably
later age. Tosephto is not merely of great help for understanding
the Mishnah, which is, in a certain sense, incomplete without it,
but for the precise and e:5act knowledge of Jewish archaeology and
other sciences, and in its Agadic parts, of which there are many, for
the Creek Scriptures also. Here ought "also to be mentioned Ahoth
dt-Rabbi Nathan, which is, no doubt, Tosephto to the Mishnah of
.Aboth. Tosephto used to bo printed till within the last forty years '
ias an appendix 'to the Miph, i.e., the Bilekhoth Bab Alphes (a
'tor.ipendium of the Talmud by E. Yitshak b. Ya'okob Al-Phesi,
or jVl-Phasi, i.e., of Fez, ob. 1103), which appeared first with this
apj. :ndix at Venice, 1521-22, folio. Here, however, it was not
cil.'.cd critically or printed with even ordinary care. But in the
Vienna edition of the Babylonian Talmud (1860-72) it came out,
for the first time, worthily after a iJS. till then uncollated which
is preserved in the Court Library. Dr Zuckermandel has since
Eablished it from the Erfurt and Vienna MSS., with collations. ° A
atin translation of Tosephto (with the Hebrew te.xt) is to be found,
under the name of To.mphia, in Blasins Ugolinus's Thesaurus
Antiquilalum Satrarum (xvii.-xx.). It comprises, however, only
the orders Zera'im, Mo'cd, and Kodoshim, and came out at Venice
in the years 1755-57, folio.
The second of these pieces of literature is MekhiUo. This word
is tlie Aramaic equivalent of the Hebrew Middah (measure), and
lience signifies mould, foi-m, i.e., of Scriptural exegesis, notably of
part or parts of the Pentateuch. As such it might, of course,
stand for any kind of commentary on any book of the Pentateuch,
and have been composed by any one. And we find, indeed, that
MekhiUo signified at one time a commentary on the hooks Exodus,
Leviticus, Numbers, and Deuteronomy, either by E. Yishma'el or by
R. 'Akibah,* at another time a commentary on Exodus, by E.
fShimc'on b. Yohai,* and at another time again a commentary on the
Last four books' of Moses, by (Shime'on) Ben 'Azzai.' MekhiUo
now, however, means a commentary on the greater part of Exodus,
ascribed to E. Yishma'el (flourished in the 1st century) ; although,
in reality, this teacher cannot have been the author of the book,
seeing that his name is more than seventy times mentioned in it.
The reason why the ancients called the book by his name is, no
doubt, because the first words of the real work are Amar Rabbi
yishma'el. Like the other works of the " oraWavr," MekhiUo vfas
not written down before the 6th century, a fact which accounts
also, in part at least, for the loss of several portions of this com-
mentary, which, at present, only extendsfrom xii. 1 to xxv. 3,
with several gaps between. That MekhiUo was once fuller than it
is now we know, not only from a statement made by Maimonides
and others, but from a MS. (Add. 394. 1, in the University Library
of Cambridge, leaf 406), where an extract is given by a Franco-
German author of the 12th or 13th century. The Talmud knows
tho namo MekhiUo, and actually quotes Boraithoth (non-canonical
Mishniyyoth) which are to be found in our book ; and yet the
existing MekhiUo can scarcely have been known to the teachers of
tho Talmud. MekhiUo is by some called Midrash and by others
Mishnah; both names arc in a certain sense correct. It is Mid-
rash in substance, inasmuch as it contains exegesis, and in form,
inasmuch as it is subdivided into Parshiyyoth and follows the order
of tho Scriptural verses. But it is Mishnah in substance, inas-
much as it not only deals with the groundwork of tho Mishnah,
but consists of Boraiihoth (non-canonical Mishniyyoth), and in
form, inasmuch as it is, like the canonical Mishnah, divided into
Massekhloth. These latter are nine in number, and are called re-
spectively (1) Dephisha (with 18 Parshiyyoth and 1 Pcthihto or
introduction), (2) SeshaUah (with 6 Parshiyyoth and 1 Peihihto),
(3) Dcihirttha (with 10 Parshiyyoth), (4) Vayyassa' (with 6 Par-
shiyyoth), {b)'Amakk (with 2 Parshiyyoth), (S) Yithro (with 2
parshiyyoth), (7) Bahodesh (with 11 Parshiyyoth), (8) NeziJcin and
Kaspo (with 20 Parshiyyoth), and (9) Shabbetho (with 2 Par-
s'tiyyoth — 1 in the pericope A't thissa and 1 in that of Vayyakhel).
jVelchiUo was published first at Constantinople in 1516, under
the name of Sephcr HammclMilio, and in 1545 at Venice as Mid-
rash HaminekhiUo. In 1712 it appeared at Amsterdam with a
commentary. In 1744 it appeared again at Venice with a Latin
translation by Blasius Ugolinus ( J'Acs. Antiq. <Sacr., xiv.). In 1801
it appeared at Leghorn with a difi'erent commentary. In 1844 it
* ' That on the order Zerdim came out at Vilna in 1799, 4to ; but
tin i^.s entirety it came only out between 1837, 1841, and 1871, folio.
■ Issued :.i Pasewalk and Troves from 1877 to 1882, 8vo.
^ See Maimonides's preface to the Mishneh Torah.
~ See Nahmanides's commentary on the Pentateuch (on Gen. xlix. 31).
* Sec Tuhasin Hasshatem (ed. FUipowski, London and Edinburgh,
•1857, 8vo),'p. 30, col. 2.
came out at Vilna with a new commentary. All these are in foliol
The best and cheapest editions with commentaries are those tj
Weiss (1865) and Friedmann (1870), both printed at A'ienna, and
in 8vo. . I
The third of these pieces of literature is Siphro. Both LeviticoA Siparo.»
itself, because it is the most difficult of all Mosaic books, and
the oldest Eabbinic commentary on it, because it is the most
diOicuIt of all commentaries on the Scriptures, have been from tinie
immemorial known under tho name of Siphro {i.e., (Ae- Book).'
This book and this comraentary are also called Torath Kohanim,
and the former is spoken of in the Talmud already as Siphro
dele Jiab.^ This latter expression has led many great men (among
others Maimonides)^ to ascribe the authorship of this commentary
to"Kab (Abba Arikho, a nephew and disciple of E. Hiyya). But
such a view is erroneous in the extreme, as the booli is, so far as
form and substance go, both older and later than Rab, paradoxical
as this statement may appear. It is older in its origin and in
its matter, for not merely do all the anon}'mous Boraithoth which
are to be found in- it belong to E. Yehudah b. Il'ai, a teacher
of the 1st century, but one of the sons of Rabbi (of the 2d
century) had actually taught another rabbi two-thirds of a third,
i.e., two-ninths, of this work.* It is later than Eab, for in it are
found one ^'authority" and several "results" of much later date
than that of this great Babylonian teacher.^'* The fact is,. the word
Bab in the phrase Siphro dcbe Bab is not a proper name at all,
but simply stands for "teacher," and debe Bab thus signifies "of
a school," a term used for any teacher and any school of any time.
Although most of the Boraithoth which it contains are as old. ts
the 1st century, this book as -such cannot have been written down
earlier than the 6th, in accordance with the treatment, in this
respect, of all the other Halakhic works of the " oral law." Siphro,
although it bears on the pericopes and verses of Leviticus, and is
on account of this fact by many called a Midrash, is in reality
Mishnah," — a name borne out hy the nature of its contents, which
are mostly Mishnic, and sometimes represent actual canonical
Mishniyyoth. Siphro exhibits a curious conglomeration of matter.
It opens with the "Rules of the Interpretation of Scripture,"
ascribed to E. Yishma'el, — a Boraitho which, although important
in itself, is not more important for this than for any other com-
mentary on the Pentateuch. And this conglomerate nature shows
itself even more strikingly in form ; for Siphro contains as forms
of division Dibburim, MekhiUo, Parshiyyoth (some of which mean
pericopes, whilst others mean chapters), Pcrakim, and Fiskoth.
All this points, of course, to various divisions of the book made at
various times. Whilst none of these divisions can be later than
the 12th century," the earliest is at least as old as the 2d, and.belonga
perhaps to the 1st." Siphro is chiefly of importance for the under-
standing of the Mishimh of the orders Kodoshimmi Tohoroth (whidi
were, no doubt, the earliest Mishniyyoth put into "order") ; bnt,
whilst it is a sure help for the Mishnah, theMishnah is no snre help
for it : Siphro is a genuine specimen of the "oral law," inasmuch
as it cannot be mastered without a teacher. Owing to the difficulty
of understanding it, Siphiro has not been often studied, and conse-
quently not often printed. The cditio princeps is of 1545 ; the
second edition with the commentary Korban Aharon is of 1609-11,
both at Venice. The third edition with the just-named commen-
tary is of 1702, and came out at Dessau. The fourth edition, with
a Latin translation, is to be lound in Blasius Ugolinus's Thesaurus
Antiquitatum Sacrarum, kc, Venice, 1744 (vol. xiv.). ' All these
are in folio. The fifth edition, with the commentary 'Azarath
Kohanim (vol. i.), appeared at Vilna, 1845, 4to. The sixth edition,
with the commentary 'Asirith Bacphah, appeared at Lemberg,
1848, folio. The seventh edition, with the commentary Ealtorah
Veham-Mitsvah, appeared at Bucharest, 1860, 4to. The eighth
edition, with the commentary of E. Abraham b. David of Pos-
quieres, 4;c., appeared at Vienna, 1862 ; and the ninth edition,
with the commentary by E. Shimshon of Sens, .appeared at War-
saw, 1866, both in folio. . .■ , ' -
The fourth of these pieces of literature is Siphcre. Siphere, or S.;)here..
Siphere debe Bab, which in earlier times certainly included the
oldest Rabbinic commentaries on Exodus, Numbers, and Deu-
teronomy (and perhaps also that on Leviticus), means now the
oldest Rabbinic commentary on the last two books of Moses only.
• See T. B., Berakhoth, ISb, and Eashi, in loeo. The Siphro said
here to have been studied by Benai.ah tho son of Jehoiada may well
have been our Leviticus, though of course it canuot have been the
Siphro with which we are here concerned.
' Ibid.
^ Preface to Mishneh Torah.
= See T. B., Kiddushin, 33a.
^^ See the pericope Kedoshim, vi.
" Its original founder (R. Yehudah b. Il'ai) identifies Mishnah ;nd
Midrash, T. B., Kiddushin, 49a.
'= They were known to R. Ati.iham b. David (Rabni^).
"T. B., Kiddushin, 3U.
\
508
M I S - M I S
Both books are divided into PtslMih (paragraph';), of which Siphere
on Numbers has 161, whilst that on Deutoronoiny has a07. The
ancient division into Boraithoth cannot now be accurately
traced. The worl'. commences now at Numbers v. 1, aud goes to
the end of Deuteronomy. The passages anonymously given in
Siph-cre are ascribed by the Babylonian Talmud ' to R. Shime'on b.
Yohai, the favourite disciple of R. 'Akibah, and the reputed author
of the Zohar. But although he is no doubt the virtual author of
Siphere, seeing that most Bomithoth which are to be found therein
are his, he cannot be, technically speaking, its author. For, in the
first place, he is not only repeatedly named in the book, but several
times actually contradicted by others ; and, secondly, there are
several passages, anonymously given, in the book, which can only
be the result of "Talmudic " study, and must be consequently pos-
terior to the composition of the Talmud. The tact is that Siphcrc,
like the other works of the "oral law," was not written down
before the 6th century. It ought to be mentioned here that the
rabbis of the 11th, 12th, and 13th centuries, and even somewhat
later, speak also of another Siphcrc which they variously designate
as Siphere Panim Sheni, Siphere shel Paiiim Shad, Siphere Bemid-
bar Sinai, Siphere ZtUta, and Siphere simply. To judge from tire
extracts which have come down to us, that work must not only
have been of much later date, but also of far less value than the work
in our hands. Siphere appearM for the first time in 1545, and with
a' Latin translation by Blasius Ugolinus, in his TJiesaurus, &c.
(vol. XV.), in 1744,— both at Venice, and in folio. The third
edition appeared at Hamburg in 1789, and the fourth at Sulzbach
in 1802, Doth in 4to. The fifth edition, with the commentary Zcra
Abraham, appeared in two volumes, of which the first was printed at
Dyhernfurt in 1811 and the second at RadaweU in 1320, both in
folio. The sixth and best edition is that of Friedmann (Vienna,
1S64), and the seventh is that of Lemherg, 1866, both in 8vo._
Bwaitho. There is also a fifth piece of Jlishnic literature known specially
Dy the name Boraiiho. Besides the Boraitholh constituting
Tosephto, ^ Mekhilto, Siphro, aud Siphere, there are hundreds of
other Boraitholh to be found scattered about in both Talmuds.
These are, however, mere fragments of the vast Mishnayoth (entire
Mishnic works") composed by Bar Kappara, Rabbi Hiyya, and
hundreds of other teachers, which in course of time must have
perished. There is, however, enough left of the Mishnah, canonical
and non-canonical, to prove the correctness of the cabbalistic
remark that MishncJi is the equivalent of Neska-mah (soul). This
is no mere trifling based on the fact that the two words (n3t;'0,
nOB'3) accidentally consist of the same letters ; it is rather an
enunciation of an intrinsic truth : what the soul {Neshamah) is to
the body, the Mishimh is to lIos.aism. Tha soul gives life to the
body, and the Jlishnah gives life to the Pentateuch. For the letter
kUleth, but the spirit giveth life ! (S. M. S.-S.)
MISKOLCZ, capital of the Cis-Tisian county of Borsoo,
Hungary (4S° 6' N. lat., 20° 49' E. long.), is picturesquely
situated in a valley watered by tlie Szinva, 90 miles north-
east from Budapest, with which, as also with Debreczen
and Kassa (Kaschau), it is directly connected by railway.
Miskolcz is one of the most thriving provincial towns in
the kingdom, and has many fine buildings, including Roman
Catholic, Greek Catholic, Lutheran, and Calvinist churches
and schools, a Minorite convent, synagogue, Hungarian
theatre, hospital, royal and circuit courts of law, salt and
tax office.?, and the administrative bureaus for the county.
There are manufactories of snuff, porcelain, boots and shoes,
and prepared leather, and both steam aud water mills. The
trade is chiefly in grain, wheaten flour, wine, fruit, cattle,
hides, honey, wax, and the agricultural products of the
neighbourhood. The great fairs, held five times a year,
are much resorted to by strangers from a distance. Not
far from the town are stone quarries and iron mines. At
the end of 1880 the (civil) population amounted to 24,343,
of whom the majority were Magj'ars by nationality.
During the 16th and 17th centuries Jliskolcz suffered much from
the desolating hordes of Ottomans who then ravaged the country,
as also from the troops of various Transylvanian princes and leaders,
especially those of George Rikdezy and Emcric Tiikolyi. In 1781,
1843, and 1847 it was devastated by fire, and on the 30th August
1878 a great portion of the town was laid in ruins by a terrific storm.
Sec HuNOARY, vol xii. p. 374.)
jnSREPRESENTATION. See Fraud.
> Sifnhedrin, 86a.
' Aocoitling to T. B., Bagigah, 14a, there existed at on« time no
loss than Bix or seven hundred MishnaJi orders.
illSSAL,^ the book containing the liturgj', or office of
the mass, of the Latin Church. This name (e.g., Missale
Gothicum, Francorum, Gallicanum Vetus) began to super-
sede the older word Sacramentart/ (Sacramentarium, Liber
Sacramentorum) from about the middle of the 8th century.'
At that period the books so designated contained merely
the fixed canon of the mass or consecration prayer
(actionem, precem canonicam, canonem actionis), and the
variable collects, secretae cr orationes super oblata, prefaces,
and post-communions for each fast, vigil, festival, or feria,
of the ecclesiastical year ; for a due celebration of the
Eucharist they required accordingly to be supplemented by
other books, such as the Antipkonarium, afterwards called
the Graduale, containing the proper antiphons (iiltroits),
responsories (graduals),. tracts, sequences, offertories, com-
munions, and other portions of the communion service
designed to be sung by the schola or choir, and the Lectioiv,
arutm {ox Epistolarium 3,XiA.Evangelisiarium)'with. the proper
lessons. Afterwards missals began to be prepared contain-
ing more or less fully the antiphons and lessons as well as
the prayers proper to the various days, and these were called
missalia plenaria. All modern missals are of this last de-
scription. The Missale Eomanuni ex decreto SS. Concilii
Tridenttni restiiulum, now in almost exclusive use through-
out all the churches of the Latin obedience, owes its present
form to the council of Trent, which among its other tasks
undertook the preparation of a correct and uniform liturgy,
and entrusted the work to a committee of its members. This
committee had not completed its labours when the council
rose, but the pope was instructed to receive its report
when ready and to act upon it. The " reformed missal '
accordingly was promulgated by Pius V. on July 14, 1570,
audits universal use enjoined on all branches of the Catholic
Church, the otJy exceptions allowed being in the case of
churches having local and independent liturgies which
had been kept in unbroken use for at least two centuries.*
It has subsequently undergone slight revisions under
Clement Vm. (1604) and Urban Vin. (1634); and various
new masses, both obligatory and permissive, universal and
local, have been added by the competent authority.
Although the Roman is very much larger in bulk than any
other liturg)', it need hardly be explained that the com-
munion office to which it relates is not in itself inordinately
long. By much the greater part of it is contained in the
"ordinary" and "canon" of the mass, usually placed
about the middle of the missal, and occupies, though in
large type, only a few pages in any printed copy. The
work owes its bulk and complexity to two circumstances.
On the one hand, in- the celebration of the sacrifice of the
mass practically nothing is left to the impulse or discretion
of the officiating priest ; everything — what he is to say,
the tone and gestures with which he is to say it, the cut
and colour of the robe he is to wear— is carefully prescribed
either in the general rubrics prefixed to the text, or in the
running rubrics which accompany it.' On the other hand,
the Roman, Uko all the Western liturgies, is distinguished
, ' Missalis (sc, liher), MissaU, from Missa ; see vol. viii. p. 652.
• The English missal consequently contiinicd to be used by English
Catholics until towards the end of the 17th century, when it was
superseded by the Roman through Jesuit influence. The Galilean
liturgy held its gi-ound until much more recently, but has now suc-
cumbed under the Ultramontanism of the bishops.
' In ftU the older liturgies the comparative absence of rubrics is
conspicuotis oud sometimes perplexing. It is very noticeable in the
Roman Sacmmcntaries, but the want is to some extent supplied by
the verj' detailed directions for a high pontifical mass in the v.arious
texts of the Ordo Romanus mentioned below. That there was no
absolutely fixed set of rubrics in use in France during the 8lh century
is shown by the fact that each priest was required to \.Tite out an
■iccount of his own practice ("libcllum onlinis") and present it fcr
approbation to the bishop in Lent (see Baluzc, Cap. Reg. Franc., l.
824. quoted in Smith's iiic(. of Chr. Anliq., ii. 1521).
MISSAL
509
from those oi tlie iiastern Church by its flezibility.
Partly by conscious effort, no doubt, but partly also by
happy accident, a -weU-marked distinctive character has
been given in one or all of the above-mentioned respects
to the office for each ecclesiastical season, for each fast or
festival of the year, almost for each day of the week ; and
provision has also been made of a suitable communion ser-
vice for many of the special and extraordinary occasions both
of public and of private life. This richness of variety is seen
not only in the collects but also in the lessons and antiphonal
parts of the service, passages of Scripture in the selection and
collocation of which an exquisite delicacy of religious and
aesthetic instinct has been for the most part strikingly shown.
The different parts of the Roman communion office are
not all of the same antiquity. Its essential and character-
istic features are most easily caught, and their rationale
best understood, by reference to the earliest Sacramentaries
(particularly the Gregorian, which was avowedly the basis
of , the labours of the Tridentine committee), to the
Gregorian Antiphonary, and to the oldest redaction of the
Ordo Romarvus.^ The account of the mass (qualiter Missa
Eomana celebratur) as given by the Sacramentarivm
Gregorianum is to th6 eflfect that there is in the first place
" the Introit according to the time, whether for a festival
or for a common day ; thereafter Kyrie Eleison. (In
addition to this Gloria in Excehis Deo is said if a bishop
jbe [the celebrant], though only on Sundays and festivals ;
but a priest is by no means to say it, except only at
tEastertide. When there is a litany (quando letania agitur)
neither Gloria in Excelsis nor Alleluia is sung.) After-
wards the Orotic is said, whereupon follows the Apostol'iu,
also the Gradual and Alleluia. Afterwards the Gospel is
read. Then comes the Offertorium,^ and the Oralio super
•oblata is said." Then follow the Sursum Corda, the Pre-
face, Canon, Lord's Prayer and "embolism" (efiPoKuTim
or insertion, Libera nos, Domine), given at full length
precisely as they still occur in the Eoman missal.
In every liturgy of all the five groups a passage similar
to this occurs, beginning with Sursum Corda, followed
by a Preface and the recitation of the Sanctus or
Angelic Hymn. The " canon " or consecration prayer,
which in all of them comes immediately after, invariably
contains our Lord's words of institution, and (except in the
Nestorian liturgy) concludes with the Lord's Prayer and
" embolism." But within this framework there are certain
differences of arrangement, furnishing marks by which the
various groups of liturgies can be classified (see vol. xiv.
p. 709 sq.). Thus it is distinctive of the liturgy of
Jerusalem that the " great intercession " for the quick and
the dead follows the words of institution and an Epiklesis
(citikXi^o'is tov TTvevfiaro^ dytov) or petition for the descent
of the Holy Spirit upon the gifts ; in the Alexandrian the
" great intercession " has its place in the Preface ; in the
East Syrian it comes between the words of restitution and
the Epiklesis ; in the Ephesine it comes before the Preface ;
while in the Roman it is divided into two, the commemora-
tion of the living being before, and that of the dead after,
the words of institution. Other distinctive features of the
Roman liturgy are (1) the position of the " Pax " after the
consecration, and not as in all the, other liturgies at a very
early stage of the service, before the Preface even ; and
(2) the absence of the Epiklesis common to all the others.'
* For the genealogical relationabipa of the Roman with other
liturgies, the reader is referred to the article Littjbot (vol. liv. 706
sq. ), where some account is also given of the three Sacratiientaries.
Tor the doctrines involved in the "sacrifice of the mass," see
Eucharist, vol. viii. p. 650 sq.
\ * Some editions do not mention the Offertory here.
' • This was one of the points discussed at the council of Florence,
asid Cardinal Bessarlon for a time succeeded in peisuading the Greeks
to give up the Epiklesis.
The words of its "canonical prayer" are of unknown
antiquity ; they are found in the extant manuscripts of the
Sacramcntarium Gelasianum, and were already old and of
forgotten authorship in the time of Gregory the Great, who,
in a letter to John, bishop of Syracuse {Pegislr. Epist., vii.
64), speaks of it as " the prayer composed by a 'scholastic' "
(precem quam scholasticus composuerat). The same
letter is interesting as containing Gregory's defence, on the
ground of ancient use, of certain parts of the Roman ritual
to which the bishop of Syracuse had taken exception as
merely borrowed from Constantinople. Thus we learn
that, while at Constantinople the Kyrie Eleison was said by
all simultaneously, it was the Roman custom for the clergy
to repeat the words first and for the people to respond,
Christe Eleison being also repeated an equal nuihber of
times. . Again, the Lord's Prayer was said immediately
after the consecration aloud by all the people among the
Greeks, but at Rome by the priest alone.
The somewhat meagre and imperfect liturgical details
furnished by the Sacranientanum Gregorianum are supple-
mented in a very full and interesting manner by the succes-
sive texts of the Ordo Romanus, the first of which dates
from about the year 730. The ritual they enjoin is that
for a pontifical high mass in Rome itself ; but the differences
to be observed by a priest "quando in statione facit missas"
are comparatively slight. Subjoined is a precis of Ordo
Romanus I.
It is first of all explained that Rome has seven ecclesiastical
regions, each with -its proper deacons, subdeacons, and acolytes.
Each region has its own day of the week for high ecclesiastical
functions, which are celebrated by each in rotation. [This accoimts
for the Statio ad S. Maviam Majorem, ad S. Crucem in Jerusalem,
ad S. Petrum, &c., prefixed to most of the masses in the Oregorian
Sacranuntary, and still retained in the " Proprium de Tempore" of
the Roman missal.]- The regulations for the assembmig and
marshalling of the procession by which the pontiff is met and then
escorted to the appointed station are minutely given, as well as for
the adjustment of his vestments " ut bene sedeant,'' when the
sacristy has been reached. He does not leave the sacristy until the
Introit has been begun by the choir in the church. Before the
Gloria he takes his stand at the altar, and after the Kiji^ Eleison
haa been sung (the number of times is left to his discretion) he
begins the Gloria in Excelsis, which is taken up by the choir. Dur-
ing the singing he faces eastward; at its close ne turns round for a
moment to say " Pax vobis," and forthwith proceeds to the Oratio.*
This finished, all seat themselves in order while the subdeacon
ascends the ambo and reads [the Epistle]. After he has done, the
cantor with his book (cantatorio) ascends and gives out the response
(Eesponsum) with the Alleluia and Tractus in addition if the season
calls for either. The deacon then silently kisses the feet of the
pontiff and receives his blessing in the words " Bominus sit in corde
tuo et in labiis tois." Preceded by acolytes with lighted candles
and subdeacons burning incense, ho ascends the ambo, where he reads
the Gospel. At the close, with tho words "Pax tibi" and
' ' Domintis vobiscum," the pontiff," after another Oratio), descends
to the " senatorium " accompanied by certain of the inferior clergy,
and receives in order the oblations of the rulers (oblationes princi-
pum), the archdeacon who follows taking their "amulas." of wine
and pouring them into a larger vessel ; similar offerings are received
from the other ranks and classes present, including the women.
This concluded, the pontiff and archdeacon wash their bands, the
offerings being meanwhile arranged by tho subdeacons on the altar,
and water, supplied by the leader of the choir (arehiparaphonista),
being mingled with the wine. During this ceremony the echola
have been engaged in singing the Offertorium; when all is ready the
pontiff signs to them to atop, and enters upon the Preface, the sub-
deacons giving the responses. At the Angelic Hymn {Samtv.s) all
kneel and continue kneeling, except the pontiff, .who rises alone
and begins the Ca^xm. At the words *' per quern base omnia " the
archdeacon lifts the cup with the oblates, and at ' ' Pax Domini sit
semper vobiscum " he gives the peace to the clergy in their order,
and to the laity. The pontiff then breaks off a particle from the
censecrat^d bread and lays it upon the altar; the rest he places on
the paten held by the deacon. It is then distributed while Agntu
Dei is sung. The pontiff in communicating puts the particle into
the cup, saying. "Fiat commixtio et consecratio corporis et sanguinis
Domini nostri Jesu Christi accipientibus nobis in vitam setemam."
Those present communicate in their order under this species also.
' Quam collectam dicunt, Ord. Rom. II.
After sia!»il:g "Cvcilo in u-u-a Dsum,"
Item, 11^
510
As the pontilT descends into the senatoriura to give the
tlie schola begins the communion Anlijihon, and contini'.js singing
the Psalm until, all the people having coramnnicatcd, they receive
the sign to begin the Oloria, after which, the verse ha\ing been
iigain repeated, tlicy stop. The celebrant, then, lacing eastward,
otTei's the Oratio ad Cojnplcndum, which being finished the arch-
deacon says to the people, " Ite, missa est," they responding with
" Deo gi'atias."
To complete our idea of the Roman communion office as it
was prior to the end of the 8th century we must now turn to
the Gregorian Antiphonarius sive Gradualis Liber ordinatus
per circulum anni, which as its name implies contains those
variable portions of the mass which were intended to be
sung by the schola or choir. It gives for each day for
which a proper mass is provided — (1) the Anfiphona (Anti-
phona ad Introitum) and Psalmus ; (2) the Rtsponsorium
and Versus, with its Alleluia and Versus ; (3) the
Offertoriuni and Versus ; (4) the Communio and Psalmus.
Some explanation of each of these terms is necessary. (1)
The word Aniip/i^m {avTL<l>o>vov, Old English Antefn,
English Anthem) in its ecclesiastical use has reference
to the very ancient practice of relieWng the voices of the
singers by dividing the work between alternate choirs. In
one of its most usual meanings it has the special significa-
tion of a sentence (usually scriptural) constantly sung by
one choir between the verses of a psalm or hymn sung by
another. According to the Roman liturgiologists it was
Pope Celestine who enjoined that the Psalms of David
should be sung (in rotation, one presumes) antiphonally
before mass ; in process of time the antiphon came to be
sung at the beginning and end only, and the psalm itself
was reduced to a single verse. In the days of Gregory
the Great the introit appears to have been sung precisely
as at present, — that is to say, after the antiphon (proper
and par excellence), the Psalmus with its Gloria, then the
antiphon again. (2) The Responsorium, like the Greek
antiphon, derives its name from the responsive manner of
singing. As introduced between the epistle and gospel it
was probably at first a comparatively long passage, usually
an entire psalm or canticle, originally given out by the
cantor from the steps from which the epistle had been
read (hence the later name Graduale), the response being
taken up by the whole choir. (3) The Offertorium and
Communio correspond to the "hymn from the book of
P.salms " mentioned by early authorities (see, for example,
Augustine, Eetr., ii. 11; Ap. Const., viii. 13) as sung
ijefore the oblation and also while that which had been
offered was being distributed to the people. A very
intimate connexion between these four parts of the choral
service can generally be observed ; thus, taking the first
Sunday in the ecclesiastical year, we find both in the
Antiphonary and in the modern Missal that the antiphon
is Ps. XXV. 1-3, the psalmus Ps. xxv. 4, the responsorium
(graduale) and versus Ps. xxv. 3 and xxv. 4, the offertorium
and versus Ps. xxv. 1-3 and Ps. xxv. 5. The communio
IS Ps. Ixxxv. 12, one of the verses of the responsorium
being Ps. Ixxxv. 7. In the selection of the introits there
are also traces of a certain rotation of the psalms in the
Psalter having been observed.
The first pages of the modern Roman missal are occupied
with the Calendar and a variety of explanations relating
to the year and its parts, and the manner of determin-
ing the movable feasts. The general rubrics {Rubricie
Getierales ^fissalis) follow, explaining what are the various
kinds of mass which may be celebrated, prescribing the
hours of celebration, the kind and colour of vestments to
be used, and the ritual to be followed (ritus celebrandi
missaui), and giving directions as to what is to be done in
case of various defects or imperfections which may arise.
The I'ra-paralio ad ilismm, which comes next, is a .short
uanual of devotion containing ps&Ims, hymns, and prayers
MISSAL
to be used as opportunity may occur before and after
celebration. Next comes the proper of the season
(Proprium Miesarum de Tempore), occupying more than
half of the entire volume. It contains the proper introit,
collect (one or more), epistle, gradual (tract or sequence),
go.=pel, offertory, secreta (one or more), communion, and
post-communion for every Sunday of the year, and also
for the festivals and ferias connected with the ecclesiastical
seasons, as well as the offices peculiar to the ember days,
Holy Week, Easter, and Whitsuntide. Between the office
for Holy Saturday and that for Easter Sunday the ordinarj-
of the mass (Ordo Misss), with the solemn and proper pre-
faces for the year, and the canon of the mass are inserted.
The proper of the season is followed by the proper of the
saints {Proprium Sanctorum), containing what is special
to each saint's day in the order of the calendar, and by the
Commune Sanctorum, containing such offices as the com-
mon of one martyr and bishop, the common of one martyr
not a bishop, the common of many martyrs in paschal time,
the common of many martyrs out of paschal time, and the
like. A variety of masses to be used at the feast of the
dedication of a church, of masses for the dead, and of votive
masses (as for thesick, forpersons journeying, for bridegroom
and bride) follow, and also certain benedictions. Most
missals have an appendix also containing certain local
masses of saints to be celebrated "-ex indulto apostolico."
Masses fall into two great subdivisions : — (1) ordinary or
regular (secundum ordinem officii), celebrated according
to the regular rotation of fast and feast, vigil and feria, in
the calendar ; (2) extraordinary or occasional (extra ordinem
officii), being either " votive " or " for the dead," and from
the nature of the case having no definite time prescribed
for them. Festival masses are either double, half-double,
or simple, an ordinary Sunday mass being a half-double.
The difference depends on the number of collects and
secretie ; on a double only one of each is offered, on a half ■
double there are two or three, and on a simple there may
be as many as five, or even seven, of each. Any mass
may be eitlier high (missa solennis) or low (missa privata).
The distinction depends upon the number of officiating
clergy, certain differences of practice as to what is pro-
nounced aloud and what inaudibly, the use or absence of
incense, certain gestures, and the like. Solitary masses
are forbidden ; there must be at least an acolyte to give
the responses. The vestments prescribed for the priest are
the amice, alb, cingulum or girdle, maniplg, stole, and
chasuble (planeta) ; see Costume, vol. vi. p. 462. There
are certain distinctions of course for a bishop or abbot. The
colour of the vestments and of the drapery of the altar varies
according to the day, being either white, red, green, violet,
or black. This last custom does not go much further back
than Innocent III., who explains the symbolism intended.
Subjoined is an account of the manner of celebrating
high mass according to the rite at present in force.
1. The priest who is to celebrate, having previously confessed (if
necessary) and having finished matins and lauds, is to seek leisure
for private prayer (fasting) and to use as he has opportunity the
" pr.ayers before mass" already referred to. How the robing in the
sacristy is next to be gone about is roiinitely prescribed, and prayers
are given to bo used as each article is put on. The sacramental
clcmentshavine previously been placed on the altar or on a credence
table, the celebrant enters the cnurch and takes his stand before
the lowest step of the altar, having the deacon on his right and the
sulidcacon on his left. After invoking the Trinity (In nomine
I'atris, ic. ) he repeats alternately with those who are withliim the
psalm " Judica me, Deus," which is preceded in the usual way by an
antiphon (Introibo ad altarc Dei), and followed also by the Gloria
and Antiphon.' The vcrsicle "Adjutorium nostrum," with its
• This antiphon is not to bo confounded with the Antip^ona ad
Introitum further on. Tliis use of the <3d Psalm goes as far back at
least as the end of the llth centurj-. being mentioned by Micrologus
(lOSO). 'It is omitted in masses for the dead and during Holy Week.
M 1 S — M I S
511
response "Qui feoit," is followed by the "Confitcor,"' said alter-
natoly by the priest and by the attendants, who in turn respond with
the prayer for divine forgiveness, "Misereatur." The priest then
gives the absolution (" Indulgentiam "), and after the versicles and
responses beginning "•Deus, tu conversus" he audibly says,
"Oremus," and ascending to the altar silently offers two short
prayers, one asking for forgiveness' and liberty of access through
Christ, and another indulgence for himself " through the merits of
thy saints whoso relics are here." Receiving the thurible from the
deacon ho incenses the altar, and is thereafter himself incensed by
the deacon. He then reads the lutroit, which is also sung by the
choir; the " Kyrie Eleison" is then said, after which the words
" Gloria in Excelsis " ^ are sung by the celebrant and the rest of the
hymn completed by the choir.
2. Kissing the nltir, and turning to the people with the formula
" Dominus vobiscum," the celebrant proceeds with the collect or col-
lects proper to the season or day, which are read secretly. The
epistle for the day is then read by the subdeacon, and is followed
by the gradual, tract, alleluia, or sequence, according to the time.*
This finished, the deacon places the book of the gospels on the
altar, and the celebrant blesses the incense. The deacon kneels
before the altar and offers the prayer "Munda cor meum,*' after-
wards takes the book from the altar, and kneeling before the
celebrant asks his blessing, which he receives with the words
" Dominus sit in corde tuo." Having kissed.the hand of the priest,
he goes accompanied by acolytes with incense and lighted candles
to tne pulpit, and with a " Dominus vobiscum " and minutely pre-
gehca dicta deleautur nostra delicta. " The celebrant then standing
at the middle of the altar sings the words " Credo in unum Deum,
and the rest of the Nicene creed is sung by the choir. *
3. With "Dominus vobiscum" and "Oremus" the celebrant
proceeds to read the Ofifertory, whicli is also sung by the choir.
This finished he receives the paten with the host from the deacon,
and after offering the host mth the prayer beginning " Suscipe,'
Sancte Pater" places it upon the corporal. The deacon then
ministers wine and the s\ibdeacon water, and before the celebrant
mixes the water with the wine he blesses it in the prayer " Deus
qui humanai." He then takes the chalice, and having offered it
(" Offerimus tibi. Domino ") places it upon the corporal and covers
It with the pall. Slightly bowing over the altar, he then offers the
prayer "lu spiritu humilitatis," and, lifting up his eyes and
stretching out his hands, proceeds with " Veni sanctiBcator."
After blessing the mcenso ("Per intercessionem bcati Michaelis
rirchangeh ) lie takes the thurible from the deacon and incenses the
bread and wine and altar, and is afterwards himself incensed as well
as the others lu their order. Next going to the epistle side of the
altar he washes his fingers as he recites the verses of the 26th Psalm
beginning " Lavabo." Returning and bowing before the middle of
the altar, with joined hands he says, "Suscipe, sancta Trinitas," then
turning himself towards the people he raises his voice a little and
says, "Orate fratres" ("that my sacrifice and yours may be
acceptable to God the Father Almighty"), the response to which
13 buscipiat Dominus sacrificiuin de manibus tiiis," to
He then recites the secret prayer or prayers, and at the end
.says with an audible voice, " Per omnia ssecula swculorum "
{£. "Amen ).
i. Again saluting with a " Dominus vobiscum," he lifts up his
hands and goes on to the " Sui-sum Corda " and the rest of the Pre-
face A different intonation is given for each of the prefaces. » At I
the Sauctus the handbell is rung. If there is a choir the Sanctus j
13 snug while the celebrant goes on with the Canon." After the ,
words of consecration of the wafer, which are said "secretly dis- i
tinctly, and attentively," the celebrant kneels and adores the
host, using elevates it, and replacing it on the corporal again '
' •*■ form very similar to the present is given by Jlicrolomis, and it '
IS foreshadowed even in liturgical hterature of the 8th century. ■
- During Lent ,iud Advent, and in masses for the de,id this is I
omitted. lu low masses it is of course said, not sung (if it 'is to be
said). It may bo added that this early position of the Gloria in I
Ktcelm 18 one of the features distinguishing Roman from Ephesine '
use. *^ [
' The tract is peculiar to certain occasions, especially of a raouniful
nature, and is sung by a single voice. By a sequence is understood a
more or less metrical composition, not in the words of Scripture, havin"
a specal bearing on the festival of the day. See, for example, thl
sequence, L.iuda Sion Salvatorem," on Corpus Christi day.
•* Ou certain days the Credo is omitted.
•» Now eleven ; they were at one time much more numerous.
The approved usagu appears to be in that case that it is sun" as
far as Hosanna m Excelsis " before the elevat.on, and " Benedictus
qui venit 18 reserved till afterwards. In France it was a very com-
mon cuatom, made general for a time at the request of Louis XII., to
"iiw •■ o salutans hostia at the elevation.
adores it (th« bell meanwhile being rung).' The same rite is
observed when the chalice is consecrated. Immediately before the
Lord a Prayer, at the words " per ipsum ct cum ipso et in ipso,"
the sign of the cross is made threo times over the chalice with the
host, and towards the close of the " embolism " the fraction of the
host takes place. After the words ■ ■ Pax Donijni sit semper vobis-
cum the emission of the particle into the cup takes place with
the words Hieo commixtio et consccratio, " ic. The celebrant
then says the Agnus Dei three times.
5 While tho choir sings the Agnus Dei and the Communion, the
celebrant proceeds, still "secrete,^' with the remainder of the office
which though printed as part of the canon is more conveniently
caUed the Communion and Post-cdmiaunion. After the praver for
the peace and unity of the church ("Domine Jesu Christc qui
dixisti I ) he salutes the deacon with the kiss of peace, saying, " Pax
tecum " ; the subdeacon is saluted in like manner, and then°conveys
the " pax " to the rest of the clergy who may be assisting. The cele-
brant then communicates under both species with suitable prayers
and actions, and afterwards administers the sacrament to the other
communicants if there be any. Then while the wine is poured into
the cup for tho first ablution he says, "Quod ore sumpsimus";
having taken it he says, ' ' Corpus tunm, Domine. " After the second
ablutionhcgoesto the book and reads the Communion. Then turn-
ing to the people with " Dominus vobiscum" he reads the Post-
communion (one or more); turnin^once more to the congregation he
uses the old dismissal formula "Dominus vobiscum " {Ji. Et cum
spiritu tuo), and "Ite, uiissa est" [or "Benedicamus Domino," in
those masses from which "Gloria in Excelsis" has been omitted]
(R. Deo Gratias). Bowing down before the altar he offers the prayer
''Placeat tibi, sancta Trinitas," then turning round he makes the
sign of the cross over the congregation with the words of the
benediction (" Benedicat ").' He then reads the passage from the
gospel of John beginning with " In principio erat Vcrbum," or
else the proper gospel of the day." (j. s. BL )
MISSIONS. The history of Christian missions may,
for practical purposes, be best divided into three chief
periods— (1) the primitive, (2) the mediiEval, and (3)
the modern. None of these periods can be neglected, for
they have an intimate connexion with each other, and
illustrate the activity respectively of individuals, of the
church in her corporate capacity, and of societies.
1. T/ie Primitive Period.
Christian missions had their origin in the example and
the command of our Lord Himself (ilatt. xxviii. 1 9) ; and
the unparalleled boldness on the part of the Founder of
Christianity, which dared to anticipate for the Christian
faith a succession of efforts which should never cease to
cause its propagation to be undertaken as "a distinct
and direct work," has been justified by the voice of history. i^'
'Whereas other religions have spread from country to
country as component parts of popular opinion, have
travelled with migration or conquest, have passed in the
train of things and by the usual channels of communica-
tion, the first foundations of the church had hardly been
laid before individual missionary activity marked the life
of each one of the circle of the apostles.
Of the actual details of their labours we have been per-
mitted to know but little. Three only of the immediate
followers of the Saviour have any conspicuous place in the
apostolic records, and the most illustrious in the whole
domain of missionary activity, St Paul, did not belong
to the original twelve. His activity took the form of
journeys and voyages, chiefly to large towns, where his
message found a point of contact either with the Jewish
synagogue or the aspirations of the Gentile world. The
result of his labours and of those of his successors
' The history of the practice of elevating the host is somewhat
obscure. It seems to have arisen out of the custom of holding up the
oblations, as mentioned in the Onlo Romanus (see above). The
elevation of the host, as at present practised, was first enjoined by
Pope Honorius III. The use of the handbell at the elevation is still
later, and was first made geueral by Gregory XI.
' The benediction is omitted in masses for the dead.
^ The reading of the passage from John on days which had not ft
proper gospel was first enjoined by Pius V.
" Davison, On Profhay, p. 278.
512
M I S S I O N ;S
was that towards the middle of the 2d century the
church had gradually extended its conquests through Asia
Minor, Greece, Italy, southern Gaul, and northern Africa.^
Ecclesiastical history can tell but little of the church's
earliest teachers, and the infancy of many of the primitive
congregations is -nTapped in hopeless darkness. Whatever
v/as effected was due to the evangelizing labours of
individual bishops and clergy, who occupied themselves "in
season and out of season," and toiled zealously and
effectively in the spread of the church, though leaving no
record of their devotion. Amongst the most distinguished
representatives of this individual activity in the 4th and
5th centuries may be mentioned Ulfila, the " apostle of
the Goths," about 325; Frumentius, a bishop of Abyssinia,
about 327 ; Chrysostom, who founded at Constantinople
in iOi A.D. an institution in which Goths might be trained
to preach the gospel to their own people ;- Valentinus, the
"apostle of Noricum," about 4i0; and Honoratus, who from
his monastic home in the islet of Lerins, about 410, sent
forth numerous labourers to southern and western Gaul,
to become the leading missionaries of their day among
the masses of heathendom in the neighbourhood of Aries,
Lyons, Troyes, Metz, and Nice.
2. The Medixval Period.
With the 5th -century the church found a very different
element proposed to her missionary energies and zeal.
Her outposts of civilization had scarcely been planted when
she was confronted with numberless hordes which had long
been gathering afar off in their native wilds, and which
were now precipitated over the entire face of Europe.
Having for some time ceased to plead for toleration, and
learnt to be aggressive, she not only stood the shock of
change but girded herself for the difficult work of calming
the agitated elements of society, of teaching the nations a
higher faith thr.n a savage form of nature worship, of
purifying and rri'ining their recklessness, independence,
and uncontrollable love of liberty, and fitting them to
become members of an enlightened Christendom.
(a) The Celtic Missionaries. — The fii'st pioneers who went
forth to engage in this diificult enterprise came from the
secluded Celtic churches of Ireland and the Scottish
Highlands, which, though almost forgotten amidst the
desolating contest which was breaking up the Roman world,
.were no sooner founded than, they sent forth "armies of
Scots " to pour back upon the Continent the gifts of
civilization and the gospel. Of many who deserve
mention in connexion with this period, the most prominent
were — Columba, the founder of the famous monastery of
lona, and the evangelizer of the Albanian Scots and
northern Picts ; Aidan,- the apostle of Northumbria ;
Columbanus, the apostle of the Burgundians of the Vosges ;
Callich or Gallus, the evangelizer of north-eastern Switzer-
land and Alcmannia ; Kilian, the apostle of Thuringia ;
and Trudpert, the martyr of the Black Forest. The
zeal of these singular men at the head of ardent disciples
seemed to take the world by storm. Travelling generally
in companies, and carrying a simple outfit, these Celtic
pioneers flung themselves on the Continent of Europe, and,
not content with rejiroducing at Annegray or Luxeuil the
willow or brushwood huts, the chapel and the round tower,
which they had left behind in Derry or in the island of Hy,
they braved the dangers of the northern seas, and pene-
trated as far as the Faroes and even far distant- Iceland.'
(6) The English Missionaries. — Thus they laid the
foundations, awing the heathen tribes by their indomitable
spirit of self-.sacrifice and the sternnes.s of their rule of life.
•Justin, Dint. c. 117; TertuU., Apot., 37; Id., Adv. Jtid., 7.
=> Theodoret, /I.E., v. 30.
' Seo A. \V. lladJ.iii, " Scota on the CouUuont," Remaint, p. 256.
But, marvellous as it was, their work lacked the element
of permanence ; and it became clear that if Europe wa5.-6)
be carried through the dissolution of the old society, and
missionary operations consolidated, a more practical system
must be devised and carried out. The men for this work
were now ready. Restored to the commonwealth of nations
by the labours of the followers of Augustine of Canterbury
and the Celtic missionaries from lona, the sons of the
newly evangelized English churches were ready to go forth
to the help of their Teutonic brothers in the German
forests. The energy which warriors were accustomed to
put forth in their efforts to conquer was now " exhibited in
the enterprise of conversion and teaching " * by Wilfrid on
the coast of Friesland,^ by Willibrord in the neighbourhood
of Utrecht,'' by the maitjT-brothers Ewald or Hewald
amongst the " old " or continental Saxons,^ by Swidbert
the apostle of the tribes between the Ems and the Yssel,i
by Adelbert, a prince of the royal house of Northumbria,
in the regions north of Holland, by Wursing, a native of
Friesland, and one of the disciples of Willibrord, in the
same region, .and last, not least, by the famous Wir'jfrid
or Boniface, -the "apostle of Germany," who went forth
first to assist WiUibrord at Utrecht, then to labour iR
Thuringia and Upper Hessia, then, with the aid of his
kinsmen Wunibald and Willibald, their sister Walpurga,
and her thirty companions, to consolidate the -work of
earKer missionaries, and finally to die a martyr on the
shore of the Zuyder Zee.
(c) Scandinavian 2IissioHS. — Devoted, however, as ware
the labours of Boniface and his disciples, the battle was
not yet nearly won. .All that he and they and the emperor,
Charlemagne after them achieved for the fierce untutored
world of the 8th century seemed to have been done in vain
when, in the 9th, "on the north and north-west the
pagan Scandinavians were hanging about every coast, and
pouring in at every inlet; when on the east the pagan
Hungarians were swarming like locusts and devastating
Europe from the Baltic to the Alps ; when on the south
and south-east the Saracens were pressing on and on \vith
their victorious hosts. It seemed then as if every pore of
life were choked, and Christendom must be stifled and
smothered in the fatal embrace."* But it was even now
that one of the most intrepid of missionary enterprises
was undertaken, and the devoted Anskar went forth and
proved himself a true apostle of Denmark and Sweden,'
sought out the Scandinavian viking in his native home and
icy fiords, and, after persevering in the face of apparently
insurmountable difficulties and hardships, handed on the
torch of self-denying zeal to others, who "casting their
bread on the waters " saw, after the lapse of many years,'
the close of the monotonous tale of burning churches and
pillaged monasteries, and taught the fierce Northman to
lay aside his old habits of piracy, and gi-adually learn
respect for civilized institutions.
(d) Slavonic Missions. — Thuo the " gospel of the
kingdom " was successively proclaimed to the Roman, tlie
Celtic, the Teutonic, and the Scandinavian world. A
contest .still more stubborn remained with the Slavonic
tribes, wth their triple and many-headed divinities, their
.powers of good and powers of evil, who could be approached
only with fear and horror, and propitiated only with
human sacrifices. Mission work commenced in Bulgarin'
during the latter part of the 9th century ; thence it
extended to Moravia, where two Greek missionaries — Cyril
and Methodius — provided for the people a Slavonic Bible
* Church, Oi/la of Civilizol'v, p. 330.'
» Bede, U.K., v. 19.
• " Aonal. Xantenses," Peril, Mon. Gertn.y it-
' Bedc, II. E., V. 10.
' See Lightfoot, A ncient and Modem .Viaioiu,
miBSIONS
613
tuxi a, Slayonic Litm-gy ; thence to Bohemia, and so
onwards tj iiio Scythian wilds and level steppes, where
arose the Russian kingdom of Ruric the Northman, and
where about the close of the 10th centiuy the. Eastern
Church " silently and almost unconsciously bore into the
world her mightiest offspring." ' But, though the baptism
of Vladimir and the flinging of the triple and many-headed
idols into the waters of the Dnieper was a heavy blow to
Slavonic idolatry, mission work was carried on with but
partial success ; and it taxed all the energies of Albrecht,
bishop of Bremen, of Viciliit, bishop of Oldenburg, of
Bishop Otto of Bamberg the apostle of the Pomeranians,
of Adalbert the martyr-apostle of Prussia, to spread the
word in that country, in Lithuania, and in the territory of
the Wends. It was not till 1168 that the gigantic foiir-
headed image of Swantevit was destroyed at Arcona,
the capital of the island of Rugen, and this Mona of
Slavonic superstition was included in the advancing
circle of Christian civilization. As late as 1230 human
sacrifices were still being ofEered up in Prussia and
Lithuania, and, in spite of all the efforts of the Teutonic
Knights to expel by force the last remains of heathenism
from the face of Europe, idolatrous practices still lingered
amongst the people, while in the districts inhabited
by the Lapps, though successful missions had been
inaugurated as early as 1335, Christianity cannot be said
to have become the dominant religion till at least two
centuries later.
(e) Moslem MissioTis. — The mention of tne order of the
Teutonic Knights reminds us how the crusading spirit had
affected Christendom, and exchanged the patience of a
Boniface or an Anskar for the fiery zeal of the warrior of
the cross. ' Still it is refreshing to notice how even now
there was found the famous Raymond Lully to protest
against propagandism by the sword, to ilrge on pope after
pope the necessity of missions amongst the Moslems, and
to seal his testimony with his blood outside the gates
of Bugiah in northern Africa (June 30, 1315). Out
of the crusades, however, arose other efforts to bear the
banner of the cross into the lands of the East, and to
develop the work which Nestorian missionaries from
Baghdad, Edessa, and Nisibis had already inaugurated
along the Malabar coast, in the island of Ceylon, and
in the neighbourhood of the Caspian Sea. Li 1245
the Roman pontiff sent two embassies, one to charge
the Mongol warriors to desist from their desolating inroads
into Europe, the other to attempt to win them over to
the Christian faith. The first, a party of four Dominicans,
sought the commander-in-chief of the Mongol forces in
Persia ; the second, consisting of Franciscans, made their
way into.Tartary, and sought to convert the successor
of Oktai-Khan. Their exertions were seconded in 1253
by the labours of another Franciscan whom Louis IX. of
France sent forth from Cyprus,- while in 1274 the
celebrated traveller Marco Polo, accompanied by two
learned Dominicans, visited the court of Kublai-Khan,
and at the commencement of the 14th century two
Franciscans penetrated as far as Peking, and kept alive a
dickering spark of Christianity in the Tartar kingdom,
even translating the New Testament and the Psalter into
the Tartar language, and training youths for a native
Diinistry.'
(/) Mission* to India and the New World. — These ten-
tative missions in the East were now to be supplemented by
others on a larger scale. In 1486 the Cape of Good Hope
was rounded by Dias, and in 1508 the foxmdations of the
• Stanley, Eastern Church, p. 294.
'Neander, vil 69; Haklayt, 171; Hue, L 207.
• Neaudei, TiL 79; Gieseler, iv. 259, 260; Haidwick, Middle Ages,
236-33^
Portuguese Indian empire were laid by Albuquerque.
Columbus also in 1492 had landed on San Salvador, and
the voyages of the Venetian Cabot along the coast of North
America opened up a new world to missionary enterprise.
These bold discoverers had secured the countenance of the
pope on the condition that wherever they might plant a
flag they should be also zealous in promoting the extension
of the Christian iaith. Thus a grand opportunity was
given toi the chmches of Portugal and Spain. But the
zeal of the Portuguese, even when not choked by the rising
lust of wealth and territorial power, took too often a
one-sided direction, repressing the Syrian Christians on
the Malabar coast, and interfering \vith the Abyssinian
Church,^ while the fanatic temper of the Spaniard,
maddened by his prolonged conflict with the iafidcl at home,
betrayed him into methods of propagating his faith which
we cannot contemplate without a shudder, consigning, in
Mexico and Peru, multitudes who ' would not renounce
their heathen errors to indiscriminate massacre or abject
slavery.^ Their only defender for many years was the
famous Las Casas, who, ha\'ing sojourned amongst them
till 1516, has drawn a terrible picture of the oppression
he strove in vain to prevent.* Some steps indeed were
taken for disseminating Christian principles, and the pope
in granting territory to the crowns of Spain and Portugal
had specially urged this duty, and had been instrumental
in inducing a band of missionaries, chiefly of the mendicant
orders, to go forth to this new mission field.' But the
results were scanty. Only five bishoprics had been
established by 1520, and the number of genuine con-
verts was small. In settling, however, his realm the
conqueror of Mexico evinced no little solicitude for the
spiritual welfare of his charge; and the labours of the
devoted men whom he begged the emperor to send out
were successful in banishing every vestige of the Aztec
worship from the Spanish settlements.'
(g) The Jesuit Missions. — It was during the period at
which we have now arrived that the great organization of
the Jesuits came into existence, and one of the first
of Loyola's associates, Francis Xavier, was also one of the
greatest and most zealous missionaries of his or any other
era. Encouraged by the joint co-operation of the pope
and of John HI. of Portugal, and strongly tinged like
Loyola with ideas of chivalry and self-devotion, he disem-
barked at Goa on the 6th of May 1542, and before his
death on the Isle of St John (Hiang-Shang), December 2,
1552, he had roused the European Christians of Goa to a
new life, laboured with singiilar success amongst the Para-
vars, a fisher caste near Cape Comorin, gathered many
converts in the kingdom of Travancore, visited the island
of Malacca, made his way to and founded a mission in
Japan, thence revisited Goa, and impelled by the quenchless
desire to unfurl the baimer of the cross in China, had set
out thither to fall a victim to malignant fever at the
early age of forty -six, within sight of that vast empire whose
conversion had been the object of his holy ambition.
The immediate successor of Xavier, Antonio Criminalis,
was regarded by the Jesuits as the first martyr of their
society (1562). Mattheo Ricci, an Italian by birth, was
also an indefatigable missionary in China for twenty-seven
years, while the peculiar methods of unholy compromise
with Brahmanism in India followed by Robert de' Nobili
drew down the condemnatory briefs of pope after pdpe, and
were fatal to the vitality of his own and other missions.
« Gtddes, History of the Chwrch of Malabar, p. 4 ; Neale, Batiem
Church, ii. 343.
• Prescott, Conquest of Mexico, i. 318, iii. 211,
• Rclacion de la Deitruycion de las Indias
' Prescott, Mexico, Ui 218 n.
• Prescott, iii. 219
XVL — 6r
514
MISSIONS
Otlier representatives of the same order worked with
success ill evangelizing the Spanish settlement of Paraguay
in 1582, while their defeated foes the Huguenots sent
forth under a French knight of Malta a body of devoted
men to attempt the formation of a Christian colony at Rio
Janeiro. By the close of the 16th century the unflag-
ging zeal of the Jesuits led to a more complete development
and organization of the missionary system of the Eoman
Church. To give unity and solidity to the work of i^issions,
a committee of cardinals was appointed under the name
of the " Congregatio de propaganda fide," and to it was
entrusted the entire management of the mission, conducted
under the superintendence of the pope. The scheme origin-
ated with Gregory XECI., but was not fully organized till
forty years afterwards, when Gregory XV. gave it plenary
authority by a bull dated June 2, 1622. Gregory's suc-
cessor, Urban YIII., supplemented the establishment of the
congregation by founding in connexion with it a great
missionaiy college, where Europeans might be trained for
foreign labours, and natives might bo educated to undertake
mission work wherever new colonies were settled. At
this college is the missionary printing-press of the Komau
Church, and its library contains an unrivalled collection of
literary treasures bearing on the particular work. From its
walls have gone forth numbers of devoted men, who have
proved themselves able to promote in a singular degree the
enlargement of the boundaries of the church by means of
material as well as spiritual forces.
3. The Modern Period.
This last period of missionai-y activity is distinguished
in a special degree by the exertions of societies for the
derelopment of mission work.
As contrasted with the colossal display of power on the
part of the Chui'ch of Rome, it must be allowed that the
chui-ches which in the 16th century broke off from their
allegiance to the Latin centre at first presented a great
tack of anxiety for the extension of the gospel and the
salvation of the heathen. The causes of this, however, are
not far to seek. The isolation of the Teutonic churches
from the vast system with which they had been bound up,
the conflicts and troubles among themselves, the necessity
of fixing their own principles and defining their own rights,
concentrated their attention upon themselves and their own
home work, to the neglect of work abroad.
Still the development of the maritime power of England,
which the Portuguese and Spanish monarchies noted with
fear and jealousy, was distinguished by a singular anxiety
fsr the spread of the Christian faith. Edward VI. in his
instructions to the navigators in Willoughby's fleet, Cabot
in those for the direction of the intended voyage to Cathay,
good old Hakluyt, who promoted many voyages of dis-
coTciy in addition to writing then- history, agree ^vith
Sir Humphrey Gilbert's chronicler that " the sowing of
Christianity nnist be the chief intent of such as shall make
ii.y attempt at foreign discover)-, or else whatever is builded
upon other foundation shall never obtain happy success
nr continuance." 'NATien on the last day of the year 1600
Queen Elizabeth granted a cliarter to George, earl of
Cumberland, and other " adventiu-ers," to bo a body-
corporate by the name of "The Governor and Company of
Merchants of London trading with the East Indies," the
e.xprcoscd recognition of hi^dier duties than those of com-
merce may by some bo deemed a mere matter of form,
and, to use the words of Bacon, " what was first in God's
providence was but second in man's appetite and intention."
Yet a keen sense of missionary duty marks many of the
chronicles of English mariners. Notably was this the case
with the estabUshmeut of the first English colony in
America, that of Virginia, by Sir Walter Raleigh. Tlie
philosopher Heriot, one of his colleagues, laboured for the
conversion of the natives, amongst whom the first baptism
is recorded to have taken place on August 13, 1587.'
Raleigh himself presented as a parting gift to the Virgini''.n
Company the sum of £100 "for the propagation of the
Christian religion " in that settlement.^ When James I.
granted letters patent for the occupation of Virginia it
was directed that the "word and service of God be
preached, planted, and used as well in the said colonies
as also as much as might be among the savages bordering
among them"; and the honoured names of Nicolas Ferrar
John Ferrar, Dr Donne, and Sir John Sandys, a pupU of
Hooker, are all found on the council by wluch the home
management of the colony was conducted.
In the year 1618 was published The True Honour of
Navigation and Navigators, by John Wood, D.D., dedicated
to Sir Thomas Smith, governor to the East India Company,
and much about the same time appeared the well-known
treatise of the famous Grotius, De Veritate Beligionis
Clirisiians, ■nTitten for the express use of settlers in distant
lands. The wants, moreover, of the North American
colonies did not escape the attention of Archbishop Laud
during his official connexion with them as bishop of
London, and he was developing a plan for promoting a
local episcopate there when his troubles began and hia
scheme was interrupted. During the Protectorate, in
1649, an ordinance was passed for "the promoting and
propagating of the gospel of Jesus Christ in New England "
by the erection of a corporation, to be called by the name
of the President and Society for the Propagation of the
Gospel in New England, to receive and dispose of moneys
for the purpose, and a general collection was ordered to be
mads in all the parishes of England and Wales; and
CromweU himself desired a scheme for setting up a council
for the Protestant .religion, which should rival the Roman
Propaganda, and consist of seven councillors and four
secretaries for different provinces.^ On the restoration of
the monarchy, thi'ough the influence of Richard Baxter
with Lord Chancellor Hyde, the charter already granted
by Cromwell was renewed, and its powers were enlarged.
For now the corporation was styled " The Propagation oi
the Gospel in New England and the parts adjacent -in
America," and its object was defined to be " not only te
seek the outward welfare and prosperity of those colonies,
but more especially to endeavoui' the good and salvation of
their immortal souls, and the publishing the most glorious
gospel of Christ among them." On the list of the
corporation the first name is the earl of Clarendon, while
the Hon. Robert Boyle was appointed president. Amongst
the most eminent of its missionaries was the celebrated
John Elict, who, encouraged by Boyle, and assisted by him
with considerable sums of money, brought out the Bible in
the Indian language in 1661-64, having revealed at the end
of the Indian grammar which he had composed the secret of
his success : "prayer and pains, through faith in Jesus Christ,
will do anything." Boyle displayed in other ways his zeal
for the cause of missions. He contributed to the expense
of printing and publishing at Oxford the four Gospels and
the Acts of the Apostles in the Malay language, and at his
death left £5400 for the propagation of the gospel lo
heathen lands.
The needs of the colonial church soon excited the attention
of others also, and great efforts were made by Bishop
Beveridgo, Archbishop Wake, Archbishop Sharpe, Bishop
Gibson, and afterwards by the philosoi>hic Bishop Berkeley,
and Bishop Butler, the famous author of the Analog;/, to
* Halvluvt, Voyaiics, iii. Si5.
= Oldy, 'Lift 0/ MalfMih, p. ns.
' Ncale, Hidorij of Xcw EmjUml, i. p. 2«0 ; Eumct, Hilton/ of
■.is own Times, i. p. 132.
MISSIO>TS
515
develop the colonial church and provide for the wants of the
indian tribes. In 1696 Dr Braj-, at the request of the gover-
ror and assembly of Maryland, was selected by the bishop of
London as ecclesiastical commiesaiy ; and, having sold his
effects, and raised money on credit, he sailed for Maryland
in 1699, where ho promoted, in various ways, the interests
of the church. Returning to England in 1700-1, and
supported by all the weight of Archbishop Tenison and
Bishop Compton, ho was graciously received by William TTT,
and received letters patent under the great seal of
England for creating a corporation by the name of the
"Society for the Propagation of the Gospel in Foreign
Parts " on the 16th of June 1701.
With the establishment of this corporation the era of
the activity of societies for carrying out mission worik may
be said to commence, though the opening of the 18th
century saw other movements set on foot for the same
object. ' Thus in 1705 Frederick IV. of Denmark founded
a mission on the Coromandel coast, and inaugurated the
labours of Ziegenbalg, Schultze, and Schwartz, whose
devotion and success told with such remarkable reflex
influence on the church at home. Again in 1731 the
Moravians illustrated in a signal degree the growing
consciousness of obligation towards the heathen. Driven
by persecution from Moravia, hunted into inountain-caves
and forests, they had scarcely secured a place of refuge in
Saxony before, " though a mere handful in numbers, yet
with the spirit of men banded for daring and righteous
deeds, they formed the heroic design, and vowed the
execution of it before God, of bearing the gospel to the
savage and perishing tribes of Greenland and the West
Indies, of whose condition report had brought a mournful
rumour to their ears." And so, literally with "neither
bread nor scrip," they went forth on their pilgrimage, and,
incredible as it sounds, within ten years they had established
missions in the islands of the West Indies, in South
America, Surinam, Greenland, among the North American
tribes, in Lapland, Tartary, Algiers, Guinea, the Cape of
Good Hope, and Ceylon.^
Such were the preparations for the more general move-
ments during the last hundred years, and the manifesta-
tion of missionary zeal on a scale to which it would be diffi-
cult to find a parallel in Western Christianity. '
The progress that has been made may be best judged of
from consideration of the following details : —
(o) At the close of the last century there were only seven
missionary societies in existence, properly so called. Of these
three only, the Society for the Propagation of the Gospel in
Foreign Parts, the Halle-Danish Society, and the Moravians, had
hecn at work for the greater part of the century, whilst four, the
Church Missionary Society, the Baptist Missionary Society, the
Ijondon Missionary Society, and the Dutch Society at Rotterdam,
began their work only in its tenth decade. To-day these seven
have, in Europe and America alone, increased to upwards of
seventy, and to these must be added, not only several inaependent
societies in the colonies, but nomerons missionary associations on a
smaller scale, the offspring of English and American societies.
(6) The following chronological lists illustrate the growth of
missionary societies in Britain and the United States : —
Great Britain and Ireland.
1631. ChrtsMui F>lth Society tor the West Indies.
i'JJS. Society for Promoting Christian Knowldge.
1701. Society for the PropaEation of the Gospel In Foreign Psrts.
1732. Moravian (Episcopal) Missions of the United Brethren.
1792. Baptist Missionary Society.
1795. London Wssionary Society.
1796. Scottish Missionary Society.
1799. Church Missionary Society.
1799, Rellgloas Tract Society.
180«. British and Foreign Bible Society.
1808. London Society for Promoting Christianity amosg the Jens
1S13. Wesleyan Missionary Society.
1817. General Baptist Missionary Society.
1823. Colonial and Continental Church Sodety.
1829. Chtirch of Scotland UiailoQ Boards.
Katlonal Bible Society of Scotland.
• Holmes, Els'.. Sketches of the Uiaiont of the United Brel'iTtn,
p. 3; Grant, Bamptm, Lecturet, p. 190.
. Trinitarian Bihle Society.
. Wesleyan Ladies' Auiiliar^' for F^malo Ednwtjon in Foreign Cotatrtei.
. society for Promoting Female Education in the East.
■ S"?"? .Sf^selon (now United Presbyteriani Foreign Ulaslonl.
. Colonial Missionary Society.
, Foreign Aid Society.
Coral Missionary Fund,
, Welsh Cttlnnistic Methodist Missionary Society
. (^lonisl Bishoprics Fond.
. Edinburgh Uedlcal Missionary Society.
Waldensian Missions Aid Fund-
. British Society lor the Propagation of the Goepel among the Jew.
. Free Church of Scotland Missions.
. Primitive Methodist African and Colonial Missions.
Methodist New Connexion in England Foreign Missions.
. South American Missionary Society.
, Evangelical Continental Society.
, Indliin Female Kormal School Society.
. Lebanon Schools.
. Presbyterian Chtirch in Enghu
. Turkish Missions Aid Society.
. United Methodist Free Churches Foreign Missions.
. Christian Vernacular Education Society for India.
, Central African Mission of the English Universitiea.
, British S)Tian Schools.
Melanesian Mission.
Ladles' Association for Promoting Fenale EdQcatlon amoDj t'ao Heathco..
, China Inland Mission.
Delhi Female Medical Mission.
, "Friends" Foreign Mission Association.
. Cape Town Aid Association.
" Friends" Mission in Syria and Palestine.
Irish Presbyterian Missions.
1876. Spanish and Portuguese Church Aid Society.
Columbia Mission.
Original Secession (Church Indian Mission.
1877. Cambridge Mission to Delhi.
leso. Clharch of England Zenana Missionary Society.
Vnite-i States of America.
17S3. Ccrporation for the Propagation of the Gospel hi Kr~ "nglaod.
1787. Society for Propagattog the Gospel among the Indi::^^ tt Bostflo.
180(». New York Missionary Society.
Connecticut Missionary Society for Indians.
1803. United States Mission to the Cherokees.
1806. Western Missionary Society for Indians.
1810. Board of Commissioners lor Foreign Missions.
1814. Baptist Mlssionaiy Union.
1819. Methodist Episcopal Church Missionary Society'.
1S33. Free-wiU Baptist Foreign Jlissionary Society in India.
1835. Foreign Missions of the Protestant Episcopal Church.
1837. Board of Foreign Missions of the Presbyterian Church
1837. Evangelical Lutheran Foreign Missionary Society.
1842. Seventh Day Baptist Missionary Society
Strict Baptist Missionary Society.
1843. Baptist Free Missionary Society.
1345. Methodist Episcopal Church, South.
1845. Southern Baptist Convention.
1346. American Mlssionaiy Association.
1867. Board of Foreign Missions of (Dutch) Reformed Ohnreh.
1S59. Board of Foreign Missions of United PresbyterLin Choitb.
American United Brethren, Moravian.
United States (German Evangelical Missionary Society.
American Mexican Association.
Indian Home Missionary Association
Indian Missionary Association.
Local Baptist Missionary Society.
Women's Union Zenana Missionary Society.
(c) At the beginning of the present century the total sum con-
tributed for Protestant missions can hardly be said to have
amounted to £60,000; in 1882 the amount raised by British con-
tributions alone to foreign missions amounted to upwards ol
£1,090,000,' thus divided :—
(anrch of England Missions £460,935
Joint Societies of Churchmen and Nonconformists. 168,320
Nonconformist Societies, English and Welsh 313,177
Scottish and Irish Societies 165,767
Roman Catholic Societies. 10,910
(d) At the same date it is calculated that there were about 5000
heathen converts tmder instruction, not counting those belonging
to ttie Roman Catholic missions. At the present day the converts
from heathenism may be estimated certainly at no less than
1,800,000, a single year (1878) showing an increase of about 60,000.
'(«) When the Society for the Propagation of the Gospel was
founded in 1701, there were probably not twenty clergymen of the
Church of England in foreign parts. The spiritual condition of
the settlers in America and elsewhere was terrible in the extreme,
and no effort was then made by the church to win over the heathen
to Christ. But now the position which the church holds in the
British colonies and dependencies and many parts of heathendom
is recognized by all In those regions where the society labours,
and which before it commenced its work were spiritnally the
"waste places" of the earth, there are, including the American
Church (the first fruits of the society's efforts), 138 bishops, more
than 6000 clergy, and upwards of 2,000,000 members of the
communion.
The above tables sufficiently indicate how varied are the
missionary agencies now at work, covering the heathen
» See Scott Robertson, Analysii of British Contributions to Foreum
Miesivm, 1883.
516
[,i i S S I O N S
world with a network of miosiou outposts, -which within
the last century have won nearly two millions of converts
to the Christian faith.
The continuity of missionary enthusiasm maintainea
through the primitive, the mediaeval, and the modern periods
of the church's history, operating at every critical epoch,
and survi\ing after periods of stagnation and depression,
is a very significant fact. It is true that other religions
have been called missionary religions, and that one of them
occupies the first place in the religious census of mankind.'
But the missionary activity of Buddhism is a thing of the
past, and no characteristic rite distinguishing it has found its
way into a second continent ; while, as for Mohammedanism,
the character of its teaching is too exact a reflexion of the
race, time, place, and climate in which it arose to admit
of its becoming universal.- These and other religions of
the far East may still maintain their hold over millions, but
it must be admitted that their prospect of endurance iji
the presence of advancing Christianity is very small and
it is difficult to trace the slightest probability of their
harmonizing with the intellectual, social, and moral progress
of the modern world. With all its deficiencies, the Christian
church has gained the " nations of the future," and whereas
in the 3d century the proportion of Christians to the
whole human race was only that of one in a hundred and
fifty, this has now been exchanged for one in five,^ and it
is indisputable that the progress of the htunan race at this
moment is entirely identified with the spread of the
influence of the nations of Christendom.
Side by side with this continuity of missionary zeal,
a noticeable feature is the immense influence of individual
energy and the subduing force of personal character.
Around individuals penetrated with Christian zeal and self-
denial has centred not merely the life, but the very
existence, of primitive, mediajval, and modern missions.
What Ulfila was to the Gothic tribes, what Columba
and his disciples were to the early Celtic missions, what
Augustine or Aidan was to the British Isles, what Boni-
face was to the churches of Germany and Anskar to
those of Denmark and Sweden, that, on the discovery of a
new world of missionary enterprise, was Xavier to India,
Hans Egede to Greenland, Eliot to the Ked Indians,
Martyn to the church of Cawnpore, Marsden to the Maoris,
Carey and Marshman to Burmah, Heber, Wilson, Milman,
and Dufi to India, Gray, Livingstone, Mackenzie, Steere,
Callaway to Africa, Broughton to Australia, Patteson to
Melanesia, Jlountain and Feild to Newfoundlaud, Crowther
to the Xiger Territory, Brett to Guiana. At the most
critical epochs such men have ever been raised up, and the
reflex influence of their lives and self-denial has told upon
the church at home, while apart from their influence the
entire history of important portions of the world's surface
would have been altered.
If from the agents themselves we turn to the work that
has been accomplished it will not be disputed that the
success of missions has been marked amongst rude and
aboriginal tribes. 'What was true in the early missions
has been found true in these latter times. The rude and
barbarous northern peoples seemed to fall like " full ripe
fruit before the first breath of the gospel." The Goths
and the Vandals who poured down upon the Roman empire
were evangelized so silently and rapidly that only a fact
here and there relating to their conversion has been
l>reserved. Now this is exactly analogous to modern
experience in the South Seas, America, and Africa.
We must here content ourselves with a cursory survey
» Mni Mullcr, Chi}>s, iv. p. 265.
^ Nowraau, Orammar of Assent, p. 424.
' Lightfpot, Coinvarative X^rogrcss of Ancient and Modtrn Miisionj,
p. 8 -
of what missionary enterprise has accomplished in those
regions and among the more civilized nations of Eastern
Asia.
Tkfi South Seas. — Thatmissious have done mucn in these regions
in suppressing cannibalism, human sacrifices, and infanticide,
humanizing the laws of war, and elevating the social condition of
women, is a fact confirmed by the rescarcnes of Meinicke, WaiU,
Gotland, Oberlander, and even of Darwin.*
In Australia work among the ahorigines, wherever it has been
zealously conducted, has boen blessed with signal success. Amongst
the Papuans the Moravian stations of Ebenezer in the district of
■Wiramera, and Ramahyuck in that of Gippsland, can point ;;o
their little villages of 125 native Christian inhabitants, their
cleanly houses^ and their well-ordered churches. In the district of
South Adelaide, nt Point Macleay, the Scottish Presbyterian MiE3i^?n
has been similarly successful, while in New Zealand the native
population was converted almost within a single generation. In tlie
islands north and north-west of Australia the Dutch missionai'tos
have been especially successful in the lilinahassa (see Celebes),
of whose 114,000 inhabitants more than 80,000 have been won
over to the Christian faith, forming 195 communities with 12:1
schools; and in southern Borneo, the Rhenish Mission in the south
and the Society for the Propagation of the Gospel in the north have
been enabled to establish themselves firmly, while the former
society has also done a great work among the Battaks in Sumatra.
'Amongst the dark-coloured races of Polynesia missionary work baa
made gieat advances through the labours of the London Missionary
Society, the "VVesIeyans, and the American Board. Making Tahiti
its basis of operations, the first-named society has carried on
missionaiy operations in the islands of Australasia, Hervey, Samoa,
Tokelau, and Kllice, while the -American Board has witnessed
equally favourable results in the Sandwich Islands, and in Micronesia
(Caroline, Marshall, and Gilbert Islands) the agents of the Hawaiian
Association are actively at work under the direction of American
missionaries. In Melanesia the Society for the Propagation of the
Gospel, the Wesleyans, the London Missionary Society, and the
Presbyterians are all actively engaged. The Fiji group stands out
as one of the most promising centres of Christian civilization, and
the governor. Sir A. Gordon, was enabled to report in 1S79 that, out of
a population of about 120,000, 102,000 are now regular worshippers
in the churches, which number 600, Vhile over 42,000 children are
in attendance in 1534 Christian day schools. The Loyalty Islands
have been occupied partly by Roman Catholic missions and partly
by tlie London Blissionnry Society, while lu the New Hebrides the
missionaries of the Free Church of Scotland and of the Presby-
terian churches of Canada, New Zealand, and Australia, in spite
of many obstacles, the unhealthiuess of the climate, and the variety
of the dialects spokeu, have upwards of 3000 natives receiving
Christian teaching, 800 communicants, and 100 native teachers.
On the islands of Banks, Santa Cruz, and Solomon, the English
Episcopal Church is achieving no 1 i ttle success, sending native youths
for months at a time to Norfolk Island to receive instruction, whence
they retuni again in order to spread the knowledge of truth at home.
These islands will ever be famous in connexion with the martyr
death of the noble Bishop Patteson.
The l/jt civilized Peoples of America. — The quiet humble labours
of the Sloravians have accomjilished much in Greenland and
Labrador, whilst among the Indians of Canada and tlie people of
Hudson's Bay the Society for the Propagation of the Gosi)el has
not laboured in vain, nor the Church Jlissionary Society in the
dioceses of Rupcrtslaud, Red River, Saskatchewan, and Moosonet.
At Columbia, on the coast of the Pacific, a practical missionary genius
named William Duncan has succeeded in ci%'ilizin" a body of Indiana
degraded by cannibalism, and at his Metlakahtla mission stands
at the head of a community of some thousand persons, which has a
larger church than is to be found between there and San Fraucisco.
Testimony to the value of the results achieved was borne in 1878
by Lord Dufforin, then governor-general of Canada, who declareil
tliat he could hanily find words to express his astonishment at what
he witnessed. Amongst the Indian tribes of the United StatM
work is carried on by the Moravians, tho American Board of Missions,
the Prcsbvterians of the North and South, the Baptists, the Eyia-
copal Metliodists, and the American Missionary Society ; and the
result is that 27,000 Indians, divided amongst tho 171 communitief
of different denominations (including the Roman Catholic) are in full
membership witli tho church, and have 219 places of worship,
besides 366 schools attended by about 12,222 Indian children. The
Chorokccs, the Choctaws, the Creeks, the Chickasaws, have their
own churches, schools, and academies, and may compare favourably
both intellectually and morally with their white neighbours in
]\lissouri, Arkansas, and Texas.* Amongst the negroes in the United
States more tlian 1000 places of worship have been built since the
last war, while tho American Missionaiy Association alone has
erected 26 academics with about 6000 stutleuts, for the purpose o(
■ Sec Christliobi Poreiyn MiuionSf p.
'/Wd.,pp. 08,
MISSION^S
517
preparing freed sltivei to be teachers and missionaries. Amongst
the Indians oa the fissequibo and Berbice in British Guiana, the
missions of the Society for the Propagation of the Gospel have been
rapidly extended, and now upwards of halt the Indian population
are members of Christian churches. In the British West Indies,
through the united labours of various missionary societies, out of
1,000,000 inhabitants upwards of 248,000 are returned as regular
membei-s of the churches, 85,000 as communicants, while 78,600
children receive instruction in 1123 day schools, ofAvhich number
about 45,000 belong to Jamaica.
Passing to the southern promontory of South America, we find
that the self-denying labours of Allen Gardiner are beginning to
justify the devotion that prompted them. The London South
American Missionary Society not only carries on its operations in
the Falkland Islands, where youths from Tierra del Fuego receive
instruction, but has founded stations in Tierra del Fuego itself, has
roused the natives of Patagonia from their spiritual deadness, and
has extended its labours even to the Indians in Brazil.
Africa. — Here there are three great regions of missionary activity,
— on the west coast, in the south, and in some parts of the east.
The largest and most fruitful mission field in "West Africa is
that of SieiTa Leone, where at least seven-eighths of the people
are now Christians, though the first mission does not date further
back than the present century;' and important results have also
been obtained iu Senegambia (on the Pon^as), in Old Calabar, and
in the republic of Liberia. On the Gold and Slave Coasts the
labours of English Wosleyan missionaries and of the North German
missionary societies have been crowned with no small success, while
the Basel Society, which celebrated its jubilee in 1878, has extended
its sphere of activity to Ashaatee, translating the Scriptures into
the native languages, and changing primeval marshes into bright-
looking Christian villages. In the Yoruba lands the Church
Missionary Society has 11 stations, 5994 Christians, and 1657
scholare, while on the Niger we are confronted with the interesting
spectacle of negro preachers and teachei-s labouring under the
coloured Bishop Crowther, carrying on a work which within the
last few years was consecrated by the blood of martyrs.
South Africa lias for some time been a centre of missionary
activity. Here thirteen British aud Continental associations have
proved that all the South African races, Hotteutots and Kaffres,
Fingoes and Bechuanas, Basutos and Zulus, are capable of attaining
a considerable degree of^ Christian civilization, and can not only be
instructed in handicraft and agriculture, but trained as ministers
and teachers. A single instance of this is afforded in British
EafTraria by the Lovcdale Institute of the Free Church of Scotknd,
where youths from all the above-mentioned tribes are taught along
with Europeans, and every Sunday sixty students proclaim the
gospel in the neighbouring villages. In the cause of mission work
here few ever laboured more zealously than the late Bishop Gray,
whose diocese, when first constituted, included the whole colony
of the Cape, but whose successor has now for his suffragans the
bishops of Grahamstown, Itaritzburg, St Helena, Bloemfontein,
Zululand, St John's, and Pretoria.
East and East Central Africa, so long neglected, is now being
rapidly occupied by missionary enterprise. Here the island of
Madagascar has been in gi-eat part evangelized, while on the island
of Mauritius the Anglican Mission has developed pre-eminent
results. On the mainland, the coast of Zanzibar calls for special
notice. Here the little island of the same name has long been the
seat of the Universities Mission to Central Africa, and the heroic
Bishop Steere has not only erected a cathedral on the site of the
former slave-mai'ket, but translated the New Testament into
Sawahili, a language which can be understood by the tribes around
the lakes, and even in Uganda.
Cliina. — "0 mighty fortress! when shall these impenetrable
brazen gates of thine be broken through?" was the mournful
exclamation of Valignani, the successor of Xavier, as he gazed in
sadness at the mountains of China. The words well express the
incredible difficulties which this largest and most thickly peopled
heathen land in the world, with its petrified constitution and
culture of three thousand years, presents in the way of missionary
effort. The country itself, the people, their speech, their manners,
their religion, their policy, seemed to unite in opposing an insuper-
able barrier, but history has to record how efforts have been made
by many bodies, and at many times, to break it down. An early
Nestorian Church established itself in the empire, but was either
uprooted, or died out in course of time. In the 16th century the
Jesuits undertook the task, and in spite of the persecutions which
they have undergone the missions of the Koman Church, with their
numerous foreign clergy and their hosts of natives of different
, ecclesiastical degrees, have attained no small measure of success.
Before the country was really opened to foreigners by the treaty
of Tientsin, pioneers proceeded thither from America, and from
&e London Missionary Society. The labours of Dr Legge
in translating and reducing to system the Chinese classics are
> See Lljhtfoot, ir>:int and Modern MUiicni, p. 10.
well known. At the present day it is estimated that there are
upwards of 29 societies at work in the country, with about 250
ordained missionaries and 63 female teachers, aud the number is
constantly increasing. These societies, of which the largest pro-
portion belong to England, aud the next largest to America, support,
it is estimated, 20 theological schools, 30 higher boarding schools
for boys with 611 scholars, 38 for giris with 777 scholars, 177 day
schools for boys with 4000 to 5000 pupils in attendance, 82 for girls
with 1307, whUe 16 missionary hospitals and 24 dispensaries are
under the direction of medical missionaries, whose work in China haa
been recognized almost from the first as the source of the greatest
blessing. The mission centres stud the east coast from Hong Kong
and Canton to the frontiers of Manchuria in the north ; thence
they advance little by little every year into the interior, while as
yet the western provinces are scarcely touched by missionary efforl
The literary labours of the various societies have been carried on
with the utmost perseverance ; and on the foundations laid by a
Morrison and a Milne later toilers have been enabled to raise a
superstructure of translations of various portions of the Bible, as
well as various Christian books and religious and general periodicals
which constitute a means of vast importance towards gradually
gaining over this land of culture. At Peking a Russian mission
has been labouring for more than one hundred and fifty years.
The Society for the Propagation of the Gospel and the Chorch
Missionary Society have lately opened up new centres in this
almost limitless country.' -;
Japan. — Of the missions in Japan it is as yet too early to fore-
cast the futiure. The signing of the commercial treaties of 1854
and 1858 with America and England was followed in 1859 by
efforts on the part of the American churches to extend a knowledge
of Christianity, and in these Bishop Williams, an accomplished
Japanese scholar, proved himself a valuable leader and guide.
Soon afterwards other societies found their way into the countiy,
and in March 1872 the first Japanese congiegation, of 11 converts,
was constituted in Yokohama. Within tne last eight years these
11 have increased to 1200, while the American missions have been
supplemented by those of the Church Missionary Society and the
Society for the Propagation of the Gospel. Nearly every mission
has what may be called a high school for girls, and these institu-
tions are very popular. Thousands of copies also of the Gospels
have been circulated in Japanese, aud representatives of nearly all
the missions are engaged in translating the entire New Testament,
while a Russo-Greek mission has established itself in the north, and
is advancing steadily, having already made about 3000 converts.*
Thus, when it is considered that in the beginning of the 17th
century the Japanese Government drove out the Portuguese and
massacred the native Catholic converts, and prohibited all Christians
under pain of death from ever setting foot in the country, and when
it is borne in mind that many of these old laws against Chiistianity
have not yet beeu repealed aud that the old distrust of strangers is
still plainly disccruible among the governing classes, it is clear that,
while there is much ground for hope, effectual results can only be
the work of time.
I-ndia. — What is tnie of China and Japan applies with tenfold
force to India. Here the results achifved resemble those wliich were
attained in the conflict between Christianity and the religion of old
pagan Rome, with its mass of time-honoured customs interwoven
with the literature, institutions, and history, of the empire.
Against the influence of presrige and settled prejudice the wave of
the gospel beat for centuiies iu vain. Slowly and gi-adually it was
undermining the fabric, but no striking results were immediately
visible. So also in India with the Hiudu jiroper Christianity has
hitherto made inappreciable progj-css, while among the mile
aboriginal or non-Aryan tribes its success has been remarkable.
IndeiJendeutly of Koman Catholic missions upwards of twenty-eight
societies are earnestly engaged in the English mission field, and the
following figm*es will give some idea of the progi'ess that has been
made during tlie last twenty or thirty yeare. In British India,
including Bunnah and Ceylon, it is estimated that in 1852 there
were 22,400 communicants and 128,000 native Christians young
and old; in 1862 these had increased to 49,681 communicants and
213,182 native ChrisriaHs; in 1872 there had been a further in-
crease to 78,494 communicants and 318,363 narive Christians, while
in 1878 the latter figures rose to 460,000. When we look at the
share that each of the societies has had iu this increase, we find
that the Societ)- for the Propagation of the Gospel and the Church
Missionary Society together have since 1850 increased in member-
ship from 61,442 to upwards of 164,000; the London Missionary
Society from 20,000 to upwards of 48,000 ; the Presbyterian
missions of Scotland, England, Ireland, and America from 800 to
10,000 ; the Basel mission in India from 1000 to 6805 ; the Baptist
missionary societies (including the American as well as the English)
from 30,000 to 90,000 ; the five Lutheran societies from 3316 to
about 42,000. In some places the jirogress made has been excen-'
= Tlie Roman Catholic Mission hail 404,530 convertj to China In 1676. ^im
jcarly increase of about 2000.
' ChrUtlleb, Foreign Mistioiu. p. 222.
518
M I S — M I S
(lonr'tlj rapid. In Cuddapuh, e.g., in the Telugu tcrntory, ths
J^ciety for the Propa^tion of tlio Gospel and the London Mission-
ary Society laboured side by side for upwards of thirty years without
winning over more than 200 converts. Then on a eudden there
sprang up a revival among the non-caste population, and the 200
became nearly 11,000. Among the Kols, after five years' waiting,
the Gossner missionaries baptised their first convei-ts in 1850; now
in the German and English stations together these amount to about
40,000. Since the famine, however, in 1873-79, the increase of new
converts has been still more rapid, and the practical experience of
the superiority of Christian pity to heathen selfishness and of the
helplessness of their heathen deities, united mth the effect produced
by persistent missionaiy labour in past ye^rs, brought thousanda
into the fold of the chmxh. Thus in the Tinnevelly district, where
the Church Missionary Society carries on its operations, upwards of
11,000 heathens applied In 1878 to Bishop Sargent and his nr.tive
clergy for instruction preparatory to baptism.^ In the same district,
in connexion with the Society for the Propagation of the Gospel,
between July 1877 and the end of June 1878 upwards of 23,564
persons betook themselves to Bishop Caldwell and his fellow-
labourors for Christian teaching. Thus the English Church mis-
sions in Tinnevelly and Eamnad received in little more than a year
and a holf an increase of 35,000 souls, ^ and the Propagation Society
is no\v proclaiming the gospel in nearly sis hundred and fifty
villages in the Tinnevelly district, amcngst not merely food-seeking
"rice Christians" but those who have had the courage to face severe
persecution for joining the Christian church. Encouraging progress
has also been made among the Santals and the Karens in Burmah
and Pegu. Speaking generally, it may be said that the largest
proportion of native converts is in the south, in the presidency of
Madras ; next to southern India the most fruitful field is Burmah,
where the American Baptist missions are carrying on a successful
work among the Karens, while the Propagation Society has founded
many schools on the Irawadi, and penetrated up to Rangoon, and
beyond British territory to Mandalay; next in point of numbers stand
Bengal and the North- West Provinces. Here the largest contingent
is supplied by the missions in Chutia Nagpur, among the aboriginal
tribes of the Kols, while the Santal mission also presents many
promising features. For the Punjab district and that of Sind,
the Church Missionary Society has planted in Lahore a flourishing
theological seminary for Christian Hindus, Sikhs, and Mohammed-
ans, and Christianity has advanced thence by way of Peshawar
into Afghanistan and Kashmir. It thus appears that by far the
greatest measure of success has been obtained amongst the aboriginal
races and those who are either of low caste or of no caste at all,
while the real strongholds of the Hindu religion and civilization
still stand out like strong fortresses and defy the attempts of the
besiegers. Still the disintegrating agency of contact with Christi-
anity is working out its slow but sure results. " Statistical facts,"
writes Sir Bartle Frere, " can in no way convey any adequate idea
of the work done in any part of ludia. The effect is often enormous
where there has not been a single avowed conversion. The teaching
of Christianity amongst 160 millions of civilized industrious Hindus
and Mohammedans in India is effecting changes, moral, social, and
political, which for este»nt and rapidity in effect are far more extra-
ordinary than any that have been witnessed in modem Europe."
"The number of actual converts to Christianity in India," says
Lord Lawrence, "does not by any means give an adequate result
of missionary labours. There are thousands of persons scattered
over India who from the knowledge they have acquired either
directly or indirectly through dissemination of Christian truth
and Christian principles have lost all belief in Hinduism and
Mohammedanism, and are in their conduct influenced by higher
motives, who yet fear to make an open profession of the change
in them lest they should bo looked upon as outcasts and lepers
by their own people." To some such a negative result may at
first sight appear discouraging ; but, read by the light of history,
it laarks p natural, almost a necessary, stage of transition from
an ancient historical religion to Christianity. The Brahma Somaj
is not the first instance where a system too vague and shadowy
and too deficient in the elements of a permanent religion has
filled the interval between the abandonment of the old and the
acceptance of a new faith. The cultured classes amongst the
GreeKS and Romans experienced in their day, after the popular
mythology had ceased to satisfy, a period of semi-scepticism before
Christianity had secured its hold. Meantime in India the indirect
a'-enciea which are at work — the results of war and conquest, of
E^uropean science and European literature, of the telegraph and
tho railway, the l)ook and the newspaper, the college and the school,
the change of laws hallowed by immemorial usage, the disregard of
time-honoured prejudices, tho very presence of Europeans in all
parts of the country— all these vanous influences are gradually
bringing about results analogous to that to which Sir James Mack-
intosh referred in a conversation with Henry Martyn, when tho
' Abstract of Church Missionary r^ocidy's Rqycrt for 1879, p. 13.
* Paport of the Propagation Socict]/ for 1879, p. 31 cq.
Oriental world waa made Greek by the Buccessors of Alexander Sn
order to make way for the religion of Christ. But when to these
indirect influences we add the effects of direct missionary instmo-
tion, of training schools like those of the Free Church of Scotland
in Madras, of Bishop Sargent in Tinnevelly, of Bishop Cotton in
the North- West Provinces, of Zenana missions now earned on on aii
extensive scale amongst the female population, of the numerons
missionary presses at work circulating thousands of copies of the
Holy Scriptures and of Christian books, it is obvious that, small
and insignificant as these agencies may seem compared with tho
magnitude of the work required to be done, there has been a
great advance made during recent years. The present century
of missions may favourably compare with the primitive and
mediceval ages of the church, and the continuity of the missionary
spirit operating, as we have seen, after long periods of stagnation
and depression is the best guarantee of its udtimate and more com-
plete success at the close ofthe present epoch, during which, to use
£arl Ritter's expression, "almost all the rivers of the earth have
begun to run in double currents, and nearly all the seas and rivers
have become the seas and rivers of civilization." (G. F; M.) i
MISSISSIPPI The territory drained by the Missis-
sippi river and its tributaries includes the greater part
of the United States of America lying between the Alle-
ghany Mountains on the east and the Kocky Mountains
on the west, and has an area (1,244,000 square miles) con-
siderably larger than all central Europe. The central artery
through which the drainage of this region passes is called
the Mississippi river for about 1300 miles above its mouth.
The name is then usurped by a tributary, while the main
The Mississippi &nd its Tiibutaries.
stream becomes known aa the Missouri. From its remote
sources in tho Rocky Mountains to the Gulf of Mexico
the total length of the river is about 4200 miles. The
other principal tributaries are the Ohio, the Arkansas, and
the Red River, but the Yazoo and the St Francis oftea
make dangerous contributions in seasons of flood.
The tables given below exhibit the hydraulic features
of the Mississippi and its principal tributaries.
Below the influx of the Ohio the Mississippi traverses
alluvial bottom lands liable to overflow in flood seasons.
The soil is of inexhaustible fertility, producing large crops
of com in the northern portion, cotton in the middle dis-
trict, and sugar, rice, and orange groves near tho mouth.
ITiese bottom lands, averaging about 40 miles in width,
extend from north to south for a distance of 500 miles,
having a general southern slope of 8 inches to the mile.
The river winds through them in a devious course for 1100
miles, occasionally on tho east side washing blufis from 100
to 300 feet in height, but usually confined by baiikB of its
own creation, wluch, as ^vith til! so.dimont-beaaing rivers
of like character, are highest near tho stream itselt The
general lateral slope towards the foot hills Ls about 6 inches
ISSISSIPPI
519
in 6000 feet, but the normal fall in the first mile is about
V feet. Thus apparently following a low ridge through the
bottom lands, the tawny sea sweeps onward with great
velocity, eroding its banks in the bends and rebuilding
them on the points, now forming islands by its deposits,
and now removing them as the direction of the flow is
modified by the never-ending changes in progress. Chief
among such changes is the formation of cut-offs. Two
eroding bends gradually approach each other until the water
forces a passage across the narrow neck. As the channel
distance between these bends may be many miles, a cascade
perhaps 5 or 6 feet in height is formed, and the torrent
rushes through with a roar audible for miles. The banks
dissolve like sugar. In a single day the course of the river
is changed, and steamboats pass where a few hours before
the plough had been at work. The checking of the current
at the upper and lower mouths of the abandoned channel
soon obstructs them by deposit, and forms in a few years
one of the characteristic crescent lakes which are so marked
a feature on the maps.
The total area of the bottom lands is about 32,000
square miles, of which only a narrow strip along the
immediate banks of the main river and of its principal
bayous and tributaries has even yet been brought under
cultivation. A proper system of protection against overflow
would throw' open 2,500,000 acres of rich sugar land,
7,000,000 acres of the best cotton land in the world, and
1,000,000 acres of corn land of unsurpassed fertility.
The work of embankment began in 1717, when the
engineer De la Tour erected a dyke or levee 1 mile long to
protect the infant city of New Orleans from overflow.
Progress at first was slow. In 1770 the settlements
extended only 30 miles above and 20 miles below New
Orleans ; but by 1828 the levees, although quite insufficient
in dimensions, had become continuous nearly to the mouth
of Red River. In 1850 a great impulse was given to
systematic embankment by the U.S. Government, which
gave over to the several States all unsold swamp and over-
flowed lands within their limits to provide a fund for re-
claiming the districts liable to inundation. The action
Trii:Uarks of the Loiccr Missiaaippi.
Mouth.
Eleration
atoya Sea.
Width
between
Banks.
MUes.
2,908
2,824
2,644
1,894
842
484
0
1,330
998
668
310
0
1,265
975
615
0
1,514
1,289
992
622
250
0
1,200
820
330
0
Feet.
8,800?
4,319
2,845
2,188
1,065
766
881
1,680
1,290
670
60S
881
1,649
699
432
275
10,000
8,672
1,658
418
.252
162
2,450
641
180
64
Feet.
1,500
1,500
2,600
3,000
3,000
120
1,200
5,000
5,000
i,'2bo
3,66o
150
6,000
6,000
1,500
1,500
1,600
2,000
2,000
800
800
Missouri —
Source
Three Forks
Fort Benton
Fort Union
Sioux City.
St Joseph
Mouth
Upper Mississippi-
Source
Swan River
St Pnu]
Rock Island
Mouth
Ohio—
Coudersport
Pittsburg
Cincinnati
Mouth
Arkansas —
Source
Cent's Fort
Great Bend
Fort Smith
Little Rock
Month
};cd River—
Ne.ir source
Preston
Shreveport
Mouth
75,000
75,000
100,000
100,000
100,000
60,000
isoiboo
70,000
70,000
70,000
40,000
40,000
Area of basin, 618,000 square miles; rainfall, 20'9
inches; annual discharge, S^^jpj billions [t.c,
3,780,000,000,000] cubic feet ; ratio between
drainage and rainfall, -f^; mean discharge per
second, 120,000 cubic feet.
Area of basin, 169,000 square miles; rainfall, 35'2
inches ; annual discharge, 3A billions cubic
feet ; ratio between drainage and rainfall, ^ ;
mean discharge per second, 105,000 cubic feet.
Area of basin, 214,000 square miles; rainfall, ^'6
inches ; annual discharge, 6 billions cubic fret ;
ratio between drainage and rainfall, -f^; mean
discharge per second, 158,000 cubic feet.
Area of basin, 189,000 square miles; rainfall, 293
inches ; annual discharge, 2 billions cubic feet ;
ratio between drainage and rainfall, -f^; mean
discharge per second, 63,000 cubic feet
Area of basin, 97,000 square miles; rainfall, 39
inches ; annual discharge, l-f, billions cubic feet ;
ratio between drainage and rainfall, -p^-^ ; mean
discbarge per second, 67,000 c\ibic feet.
The LoKa- lfississi]>pi.
Water Fall per
Elevation MUc.
above Sea.
Least Low
Tntci- Bcptli
upon the
Area of Cross
Section at
High Water.
Mouth of Missouri .
St Louis
Cairo
Columbus
ilcmphis
Gaines landing
Xntchez.
Red River landing. .
Baton Rouge
Donalilsouville
CarroUton
Fort St Philip
Head of Passes
Gulf
Miles.
1,286
1,270
1,097
1,076
872
647
378
316
245
193
121
37
17
Feet.
416-0
408-0
322-0
310-0
221-0
149-0
65-0
49-5
33-9
25-8
15-2
6-2
2-9
Feet
0-500
0-497
0-571
0 436
0-320
0-309
0-266
0-220
0-156
0-147
0-119
0115
0171
4,470
2,470
6-0
6 0
37-0
51-0
47-0
40-0
51-0
44-3
31 1
191,000
199,000
200,000
199,000
Drainage area,
1,244,000 • square
mile^ rainfall, 30-4
inches;aiiuualdis-
charge (including
three outlet bay-
ous), 21r3'''l''ons
of cubic feet : ratio
between drainage
and rainfall, ^i^;
mcandischarge per
second, 675,000
cubic feet.
.520
ISSISSIPPI
resulting from this caused alarm in Louisiana, for the great
bottom lands above were believed to act as reservoirs to
receive the highest flood wave j and it was imagined that
if they were closed by levees the lower country would
be overwhelmed whenever the river in flood rose above
its natural banks. The aid of the Government was in-
voked, and Congress immediately ordered the necessary
investigations and surveys. This work was placed in
charge of Captain (now General) Humphreys, and an
elaborate report covering the results of ten years of investi-
gation was published just after the outbreak of the civil
war in 1861. The second of the tables given above, and
indeed most of the physical facts respecting the river, are
quoted from this standard authority.
To understand the figures of the table it should be noted
that at the mouth of Red River, 316 miles above the passes,
the water surface at the lowest stage is only 5-^ feet above
the level of the Gulf, where the mean tidal oscillation is
about 1-j^ feet. The river channel in this section is there-
fore a freshwater lake, nearly without islands, 2600 feet
wide and 100 feet deep along the deepest line. At the
flood stage the surface rises 50 feet at the mouth of Red
River, but of course retains its level at the Gulf, thus giving
the head necessary to force forward the increased volume
of discharge. Above the mouth of Red River the case
i.4 essentially different. The width increases and the depth
decreases ; islands become numerous ; the oscUlation be-
tween high and low water varies but little from 50 feet
until the mouth of the Ohio is reached — a distance of
about 800 miles. Hence the general slope in long distances
is here nearly the same at all stages, and the discharge
is regulated by the varying resistances of cross section, and
by local changes in slope due to the passage of flood waves
contributed by the different tributaries. The effect of
these different physical conditions appears in the compara-
tive volumes which pass through the channel. At New
Orleans the maximum discharge hardly reaches 1,200,000
cubic feet per second, and a rising river at high stages
carries only about 100,000 cubic feet per second more than
when falling at the same absolute level ; while just below
the mouth of the Ohio the maximum flood volume reaches
1,400,000 cubic feet per second, and at some stages a
rising river may carry one-third more water than when
falling at the same absolute level.
/The percentage of sedimentary matter carried in suspen-
sion by the water varies greatly at different times, but is
certairdy not dependent upon the stage above low water.
It is chiefly determined by the tributary whence the water
proceeds, but is also influenced by the caving of the banks,
which is always excessive when the river is rapidly falling
after the spring flood. In long periods the sedimentary
matter is to the water by weight nearly as 1 to 1500, and
by bulk as 1 to 2900. The amount held in suspension
and annually contributed to the Gulf constitutes a prism
1 mile square and 2G3 feet high. In addition to this
amount a large volume, estimated at 1 mile square and
27 feet high annually, is pushed by the current along the
bottom and thus transported to the Gulf.
The mean annual succession of stages for long periods
is quite uniform, but so many exceptions are noted that
no definite prediction can safely be made for any particular
epoch. The river is usually lowest in October. It rises
rapidly until checked by the freezing of the northern
tributaries. It begins to rise again in February, and attains
its highest point about the 1st of April. After falling a few
fec-t it again rises until, early in June, it attains nearly the
same level as before. After this it rapidly recedes to low-
water mark. As a rule the river is above mid-stage from
January to August inclusive, and below that level for the
remainder of the year.
It has been established by measurement and observatiotf
that the great bottom lands above Red River before the con-
struction of their levees did not serve as reservoirs to
diminish the maximum wave which passed througk'
Louisiana in great flood seasons. They had already become'
filled by local rains and by water escaping into them from
the Mississippi through numerous bayous, so that at the
date of highest water the discharge into the river near their
southern borders was fully equal to the volume which the
wave had lost in passing along their fronts.
In fine, the investigations between 1850 and 1860 estab-
lished that no diversion of tributaries was possible ; that no
reservoirs artificially constructed could keep back the spring
freshets which caused the floods ; that the makipg of cut-
offs, which had sometimes been advocated as a r/ieasure of
relief, so far from being beneficial, was in the highest degree
injurious ; that, while outlets within proper limits were
theoretically advantageous, they were impracticable from
the lack of suitable sites ; and, finally, that levees properly
constructed and judiciously placed would afford protectioa
to the entire alluvial region.
Dm-iiig the civil war (1861-65) the artificial embanjiments
were neglected ; but after its close large sums were expended by the
States directly interested in repairing them. The work was done
mthout concert upon defective plans, and a great flood early in
1874 inundated the country, causing terrible suffering and loss.
Congress, then in session, passed an Act creating a commisflion of
five engineers to determine and report on the best system for the
permanent reclamation of the entire alluvial region. Their report,
rendered in 1875, endorsed the conclusions of that of 1361, and
advocated a general levee system en each bank. This system
comprised — (1) a main embankment raised to specified heights
sufficient to restrain the floods; and (2), where reasonable security
against caving required considerable areas near the river to be
thrown out, exterior levees of such a height as to exclude ordinary
high waters but to allow free passage to great floods, which as a
rule only occur at intervals of five or six years. The back country
would thus be securely protected, and a safe refuge would be pro-
vided for the Inhabitants and domestic animals living upon the
portion subject to occasional overflow. An engineering organiza-
tion was proposed for constructing and maintaining these levees,
and a detailed topographical survey was recommended to determine
their precise location. Congress promptly approved and ordered
the survey ; but strong opposition on constitutional grounds was
raised to the construction of the levees by the Government.
In the meantime complaints began to be heard respecting the
low-water navigation of the river below the mouth of the Ohio.
Forty-three places above the mouth of Red River aftorded depths
of less than 10 feet, and thirteen places depths less than 5 feet, the
aggregate length of such places being about 150 miles. A board
of five army engineers, appointed in 1878 to consider a plan of
relief, reported that 10 feet could probably be secured by narrow-
ing the wide places to about 3500 feet with hurdle work, brush
ropes, or brush dykes designed to cause a deposit of sediment,
and by protecting caving banks, when necessary, by such light and
cheap mattresses as experience should show to be best spited to the
work. Experiments in these methods were soon begun upon the
river above Cairo, and have since proved of decided benefit.
In June 1879 Congress created a commission of seven members
to mature plans to correct, permanently determine, and deepen the
channel, to protect the banks of the river, to improve and give
safety to navigation, to prevent destructive floods, and to promote
and facilitate commerce, tip to 1882 appropriations amounting
to £1,285,000 were made to execute the plans of this commission,
but with provisos that none of the funds were to be expended
in repairing or building levees for the protection of land against
overflow, although such levees might be constructed if necessary
to deepen the channel and improve navigation. Acting under this
authority, the commission have allotted considerable sums to repair
existing breaks in the levees; but their chief dependence- is upon
conti-acting the channel at low water by promoting lateral deposits,
and upon protecting the high-water banks against caving by mats of
brush, wire, &c., ballasted where necessary with stoue, — substan-
tially the plans proposed by the army board of 1873.
The bars at the efflux of the passes at the mouth of the Mississippi
have long been recognized as serious impediments to commerce.
The river naturally discharges through three principal branches, the
south-west pass, the south pass, and the north-east JJass, the latter
through two channels, the most northern of which is called Pass h
rOutrc. The ruling depth on the several bars varies with the
discharge over them, which in turn is controlled by the successive-
advances of the passes. In the natural condition the greateat
MISSISSIPPI
521
depth docs not u.tceed 19 or 13 feet. Tho first appropriation by
Congress to secure increased deptli was made in 1837, and was ex-
ponded ia an elaborate survey and in a system of dredging by
buckets, bat the plan of a ship canal was also discussed. At the
next appropriation, made in 1852, a board of officers, appointed
by the war department, recommended trying in succession — (1)
stirring up the bottom by suitable machinery, (2) dredging by
buckets, (3) constructing parallel jetties 5 liules -long at the
south-west pass, to be extended as found necessary, (4) closing
lateral outlets, and (5) constructing a ship canaL A depth of 18
feet was secured by the fii«t plan, and was maintained until the
available funds were exhausted. Under the next appropriation
(1856) an abortive attempt was made to apply tho plan of jetties
to the south-west pass. This failed from defects in execution by
the contractors, but a depth of 18 feet was finally secured by dredg-
ing and scraping. The report of 1861 discussed the subject of bar
formation at length. Although it approved the plan of jetties and
closure of outlets as correct in theory, the stirring up of the bottom
by scrapers during the flood stages of the river (six months annually)
was recommended by it as the most economical and least objection-
able. After the war this recommendation was carried into effect
for several years with improved machinery, giving at a moderate
aimual cost a depth at times reaching 20 feet at extreme low water,
but experience indicated that not much mor» than 18 feet could be
steadily maintained. This depth, entirely satisfactory at first, soon
became insufficient to meet the growing demands of commerce, and
in 1873 Major Howell, the engineer in charge, revived the pro-
ject of a ship canal. The subject was discussed carefully by a board
of army engineers, the majority approving a ship canal. In 1874
Congress constituted a special board which, after visiting Europe
and examining similar works of improvement there, reported
in favour of constructing jetties at the south pass,. substantially
upon the plan used by ilr Caland at the mouth of the Meuse ;
and in March 1875 Captain J. B. Eads and associates were authorized
by Congress to open by contoact a broad and deep channel through
the south pass upon the general plan proposed by this board. This
contract called for ' ' the maintenance of a channel of 30 feet in depth
and 350 feet in width for tv.-enty yeai-s " by " the construction of
thoroughly substantial and permanent works by which said channel
may be maintained for all time after their completion." The jetties
were to be notless than 700 feet apart. The sum of £1,080,000 was
to be paid for obtaining this channel, and £412,000 for maintaining
it for twenty years. In addition, tho contractors were authorized to
use any materials on the public lands suitable for and needed in tho
work. The south pass was 12^ miles long. It had an average width
of 730 feet and a minimum interior channel depth of 29 feet. The
distance ii'om the 30-foot curve inside the pass across the bar to
the 30-foot curve outside was 11,900 feet. The minimum depth at
average flood tide on the bar was about 3 feet. The discharge at
the mouth was about 57,000 cubic feet of water per second, trans-
porting annually about 22 million cubic yards of sediment in sus-
pension to the Gulf. A small island and shoal existed at the head
of the pass, the channel there having a minimum depth of 17 feet.
The work was begun on June 2, 1875, and has been so far success-
ful that during the year ending June 30, 1882, a channel was main-
tained having a least depth of 30 feet between the jetties and extend-
ing through the bar. Its least width was 20 feet, the average
being 105 feet The 26-foofchannel had a least width of 200 feet,
except for a few days. In the pass itself the 26-foot channel had
a least width of 50 feet. A very powerful dredge-boat was at work
between and beyond the jetties 87 days, of which 51 were devoted
to tho channel in the Gulf. A deepening of 6 feet has occurred
in Pass k I'Outre near its head since 1875. Up to the present
time the work has proved of great benefit to the commerce of New
Orleans.
For further details, see Eiver Engineering (H. L. A. )
Hatev:. mSSISSIPPI, one of the Southern States of the
American Union, derives its name from the river which
for more than 500 miles forms its western boundary
between the 35th and 31st parallels of north latitude,
separating it from Arkansas and Louisiana. The boundary
with the latter State is continued along the 31st parallel,
for 110 miles, to the Pearl river, and then down the Pearl
to its mouth. The Gulf of Mexico, eastward from the
mouth of Pearl river, completes the southern boundary.
On the north the 35th parallel, from the Jlississippi river
to the Tennessee, separates the State from Tennjssee, and
the boundary then follows the latter river to the mouth
of Bear Creek, in 34° 53' N. lat. and 88° 15' W. long.
The eastern boundary of the State, separating it from
Alabama, follows a line drawn from the mouth of Bear
Creek about seven degrees west of south to what was
" the north-western comer of Washington county on the
Tombigbee," and thence due south to the Gulf of Mexico.
Ship, Horn, Cat, and Petit Bois Islands, and those nearer
the shore, form a part of Mississippi. The extreme length
of the State, north and south, is 330 miles, and its
maximum breadth is 188 miles. Under the United States
surveys, begun in 1803, the State has been divided into
townships and sections, except such parts as were at the
first owned by individuals. The area of the State is given
in the census reports for 1880 as 46,340 square miles.
Topography. — There are no mountains in Mississippi,
but a considerable difference of level exists between the
continuously low, flat, alluvial region lying along and
between the Mississippi and Yazoo rivers, called "the
Bottom," and nearly all the remainder of the State, which
is classed as upland. The latter part, comprising five-
sixths of the whole, is an undulating plateau whose general
elevation above the water of the Gulf of Mexico increases
to 150 feet within a few miles of the coast, and varies
elsewhere from 150 to 500 or 600 feet. Some exceptional
ridges are probably 800 feet high. The streams of thi.n
region flow in valleys varying in width from a few hundred
yards to several miles. The fall of each river is not great,
and is quite uniform. Usually a considerable part of the
valley of each larger stream is several feet above its present
high water mark, and forms the " hommock," or " second
bottom " lands. On some of the rivers the lowest part of
the valley, subject to overflow, is several miles in width,
and bears a resemblance to the Mississippi Bottom
Ridges or plateaus everywhere in the upland region
divide the contiguous basins of creeks and rivers, descending
more or less abruptly to their valleys. In the north-eastern
part of the State, almost level prairies cover large areas
overlying a Cretaceous formation called Rotten Limestone.
A line of abrupt bluffs, extending southward from the
north-west corner of the State, divides the upland region
from the Bottom, where the general surface lies below
the high-water level of the Mississippi river. A few low
ridges, running north and south, and embracing about
200,000 acres, are barely above high water. The culti-
vated lauds in the Bottom lie on these, and on the borders
of the rivers and the numerous lakes and bayous, where
the surface is slightly elevated. Low swamps or marshes,
in which flourish large cypress trees (Taxodmm distichum),
lie between the streams, and frequently receive the surface
drainage from their banks. Large forest trees and dense
cane-brakes (Arundinaria gigantea) occupy the drier
ground. The Mississippi river is prevented from flooding
the Bottom during high water by a system of levees or
embankments built by a fund derived partly from taxation
on the land and partly from the proceeds of tlie sale of
public lands in the State classsd as " swamp lands," which
were given over for this purpose by Congress. The only com-
pensation for the injury done when breaks in the levees
(" crevasses ") occur is the deposit of alluvial matter left by
the overflow, which adds to the productiveness of the
already wonderfully fertile soil. The present levee system
usually protects about one-fourth of the 4,000,000 acres
in the Bottom. Many crescent-shaped lakes (" cut-ofis ")
occur in the Bottom. Similar phenomena present them-
selves in the channels of the other rivers having wide
bottoms.
The volume of water in the streams varies greatly during
the year, and is usually largest between the months of
January and April. During high water all the larger
streams are navigable by steamboats. These ply upon the
Mississippi, Tennessee, and Yazoo rivers throughout the
whole year. The rivers flowing into the Gulf are macb
obstructed by sand-bars, and are chiefly used for floating
logs to the saw-mills on the coast.
XVI. — 66
522
ISSISSIPPI
"Hie best and only deep harbour on the coast is the well-
protected roadstead inside of Ship Island. It has a depth
of 27 feet, a firm clay bottom, and is readily accessible to
lighters from the shallower harbours along the coast.
Climate. — Near the waters of the Gulf of Mexico the clima*o u
mQch milder than in the northern jparta of the State. Oa the
aonthern borders the temperature rarely falls to 32" Fahr. , or exceeds
96°, the annual mean being about 68°. The orange, lemon,
almond, baiiana, and olive can be gi-own without protection. In
the latitude of Vicksburg the temperature ranges from 98° to 20°,
Tery rarely lower j the annual mean is 65°. The range in the
northern pai-t of the State is from 98° to 15°, or rarely 10 , and the
annual mean la 61°. The fiist and last hoar-frosts ocom-, in the
central parts' of the State, usually in the latter parts of October and
March. The ground is seldom fro2en to the depth of 3 inches, and
only for a few days at a time. The rainfall on the coast is 60 to 65
inches per annum, and at the northern boimdary 50 inches. "While
about two-thirds of this precipitation occm-s in winter and spring,
a month seldom passes without several inches of rainfall.
Land and sea breezes in the south, ;!ud variable winds elsewhere,
make the heat of summer tolerable. In healthfulness Mississippi
compares favourably with other States. The average death-rate of
thirteen States, variously situated, as given in the census of 1880,
is 1 '38 per cent. ; that of Mississippi is 1 -19 per cent. Where the
surface is flat and poorly drained malarial fevei-s are prevalent daring
the warm season. Yellow fever has become epidemic after importa-
tion, but strict (^uarautine has been successful in preventing it.
Geology. — In accordance with an Act of the legislature passed in
1850, an agricultural and geological survey of the State was begun,
which contiiiued, with interruptions, until 1871. Two reports have
been published, one in 1854 and another in 1860.
The geological structure of the State is comparatively simple,
and closely related to that of the adjacent States. The older
formations are nearly all overlaid by deposits of the Quatei-nary
period, which wUl be described last. In the extreme north-
eastern portion are found the oldest rocks in the State, — an ex-
tension of the Subcarboniferons formation which underlies the
'Warrior coal-fields of Alabama. The strata here show some traces
of the\ upheaval which formed the Appalachian mountain chain,
whose south-west termination is found in Alabama. "When this
chain formed the Atlantic mountain-border of the continent, except-
ing this north-east comer, Mississippi had not emerged from the
•waters of the ancient Gulf of Mexico. As the shore-line of the
Gulf slowly receded southward and westward, the sediment at its
bottom gradually came to the surface, and constituted the Cretaceous
and Tertiary formations of this and adjacent States. "Wherever
stratification is observed in these formations in Mississippi, it
shows a dip west and south of 20 or 30 feet to the mile. The
Cretaceous region includes, with the exception of the Subcarboni-
ferons, all that part of the State eastward of a line cutting the
Tennessee boundary in 89° 3' "W. long., and drawn southward
and eastward through the towns of Kipley, Pontotoc, and Stark-
ville, crossing into Alabama in latitude 32° 45'. Four groups of
Cretaceous strata have been determined in Mississippi, defined by
lines having the same general direction as the one just described.
The oldest, bordering the Subcarboniferous, is the Eutaw Oj:
Cofiee group, characterized by bluish-black or reddish laminated
clays, and yellow or grey sands, containing lignite and fossil resin.
"Westward and southward to the city of Columbus ia the
Tombigbee sand group, consisting chiefly of fine-grained micaceous
sands of a greenish tint, with many marine fossils. Next in
order, westward and southward, is the Rotten Limestone group,
made, up of a material of great uniformity, — a soft chalky rock,
white or pale blue, composed chiefly of tenacious clay, and white
carbonate of lime in minute crystals. Borings show the total
thickness of this group to be about 1000 feet. Fossils are abundant,
but species are few. The latest Cretaceous is the Ripley group,
lying west of the northern part of the last-named fTOup, and
characterized by hard crystalline white limestones, and dark-
coloured, micaceous, glauconitic marls, whose marine fossils are
admirably preserved. One hundred and eighty species have been
described. The total thickness of the Cretaceous is abont 2000
feet. Deposits of the Tertiary period form the basis of more than
half the State, extending from the border of the Cretaceous west-
ward nearly or quite to the Yazoo and Mississippi Bottom, and
southward to within a few miles of the Gulf coast. Seven groups
of the Tertiary strata have been distinguished. Beginning nearest
the Cretaceous, the Flatwoods group is characterized by grey or
white clays, and a soil which responds poorly to tillage. The
Lagrange group, lying to vho west of the last, is marked by grey
clays and sands, fossil plants, and beds of lignite or brown coal,
sometimes 8 feet in thiclcness. Tlie Buhrstono group, lying soutb-
westw.ird from the last, is characterized by beds of white siliceous
clays, and of silicified shells, and sandy strata containing glauconite
in valuable quantities. The Claiborne group lies south of the
last, and is slightly developed in Mississippi, but well-marked in
Alabama. The Jackson group, sonth-west of tlia last two, is
made up chiefly of soft yellowish limestones or mark, containing
much clay, and sandy strata with glauconite. Zenglodon bones
and other marine fossils are abundant The Vicksburg group Uea
next in order south-westward, and is characterized by crystalline
ii'nestones and blue and whito marls. Marino fossils ai-c very
abundant. More than one hundred and thirty species have been
determined. The Grand Gnlf group, showing a few fossil plants
and no marine fossils, extends southward from the last to within
a few miles of the coast.
The oldest formation of the Quo ternary period is the "orange
sand" or "stratified drift," which immediately overlies aU the
CretaceoQs groups except the prairies of the Rotten Limestone,
and all the Tertiary except the Flatwoods and Vicksburg groups
and parts of the Jackson. Its depth varies from a few feet to over
200 feet, and it forms the body of most of the hills in the State.
Its materials are pebbles, clays, and sands of various colours from
white to deep red, tinged with peroxide of iron, which sometimes
cements the pebbles and sands into compact rocks. The shapes of
'P' T j: sr N E s s eve_
^[■■-r r?"(s^yjV"\^
Geological Map of Mississippi State,
these ferruginous sandstones are very fantastic, — tubes, hollow
spheres, plates, &c., being common. The name stratified drift is
used by the geologist of Alabama to indicate its connexion with
the northern drift. The fossils are few, and in some cases probably
derived from the underlying formarions. "Well-worn pebbles A
amorphous ijuartz, agate, chalcedony, jasper, &c., arc found in the
str.^tified drift along the western side of the Tertiary region of
the State, and from Columbus northward. ""While this forma-
tion is not well understood, it seems tolerably well established
that the melHng of the great glaciers of the north furnished the
water which brou^t with it fragments of the rocks over which
it passed, and flowed into the Gulf with a current which was
most rapid where the pebbles were dropped, but overspread tiie
remainder of the State with a gentler flow, leaving sands and
clays " {E. A. Smith). The second Quaternary formation ia the
Port Hudson, occurring within 20 miler of the Gulf coast, and prob-
ably outcropping occasionally in the Mississippi Bottom. Clay!?,
gravel, and sands, containing cypress stumps, drift-wood, anl
mastodon bones, are characteristic. Tho loess or bluff fomiatica
lies along the bluffs bordering the Bottom, nearly continuously
through tho Stato. Its fine-grained, unstratified silt contains the
remains cf many torrostrial animals, including fifteen niaiomals.
MISSISSIPPI
523
The sorfaco and subsoil of nearly all the upland region of
Ui^isaippi, the southern part being the eicej)tion, is composed of
yellow foam or brick-clay containing no fossils, and showing no
stratification. The soil of the Rotten Limestone region is similar in
ka general make up, but is black, and contains more lime and
clay. Both are regarded as an independent aqueous deposit, pos-
terior to the stratified drift and bluff formations, and anterior
to the alluvium of the present epoch. The *' second bottoms,"
probably, are later than the yellow loam, and belong to the " terrace
epoch." The latest fonaation, alluvium, is stronyly inarked, and
oorero a large area iu the Yazoo and Mississippi Bottom, and along
other streams.
The following are the eqtuvalents of the Mississippi groups in
Dana's Geology : —
Qoatenury.
Cnitaceons.
F 20c Xx>ainan4 loess Loam aad loess.
"1 20& Port Hodson «. Port Uadson.
(.20a DrifC. .r. SR-atillea dilit,
1- Doner ( Grond Gait
Jackson.
Claiborne.
Lower i Euhrstone, Lagrange.
"^f- I Rotten Limestone
Lo«r lll^^l^"''-
• I Coffee.
SiibcarbODifeFOOs Keokuk.
Minerals. — Metallic ores are not found in Mississippi in paying
quantities. The only valuable minerals are sandstones and lime-
stones, marls, sands, lignite or brown coal, and fire-clays. None of
these have been extensively brought into market. Potable water is
found almost everywhere. Artesian wells furnish it in the Rotten
Limestone region, when bored into the underlying Coffee strata.
J^aunn. — Mississippi affords perhaps no species which are not
found in the neighbouring States. There are thirty or forty species
of MamiTialia, the most remarkable being the American opossum,
sriU quite abundant. The deer((?ermw virginianus), black bear
ll7rsiis americantis), wolves (Canis lupus &ui. iMpus amerkanus),
ratsmount {Felis concolor), and wild-cat {Lyncus rw/us) have much
;Iocreased in number, and may, like the buffalo and elk, shortly
K-ecomo extinct. About one hundred and fifty species of birds
ire found during at least part of the year. Many are seen only
in transHUj and about twenty species from the north spend the
vTinter here. The mocking bird {Mitnus poli/gloitus), the most
remarkable songster, is very abundant. The wild turkey {Ifeleagris
■jallipavo) survives by virtue of its wary and watchful character.
Over fifty species of SepHlia have been found, prominent among
wliich is the alligator (A. mississippimsis), which attains a length
o( 12 or 15 feet, and is common in the southern river bottoms.
The rattlesnake, moccasin^ and copperhead, venomous serpents, are
occasionally found. About half of the sixty-three species of fish
abounding in the fresh and salt waters of the State are valuable
ibr food. The edible oysters and crustaceans of the coast are
lemarkably fine.
Flora. — Originally nearly the entire State was covered with a
growth of forest trees of large size, mostly deciduous. The under-
yrowth was kept down by annual burnings by the natives, and
me ground became carpeted with grasses and herbs. Over 120
species of forest trees are found ; many valuable ones are abundant,
and their timber constitutes a large item in the resources of the
State. Of the 15 species of oak the most valuable are the live-oak
(C. virens), found near the coast, and the white-oak {Q. alba),
widely distributed. The cypress {Taawdium distichum) is very
abundant in the bottoms. Various species of hickory, the chest-
nut, black walnut, sweet gum, cucumber tree, Cottonwood {Populus
deltoides), red cedar, elms, holly, magnolias, maples, ash, persim-
mon, sycamore, tupelo, and many others valuable for their timber,
are abundant and of large size. The long-leaved pine {P. australis)
forms the principal forest growth south of lat. 32° 15'. It. attains
a diameter of 2 or 3 feet, has a tall and shapely trunk, and its
'. imber is unsurpassed in the variety of its uses. The census reports
estimate the merehantable timber of this species now standing in
the State at 18,200,000,000 feet, board measure. The amount cut
ia 1880 was 108,000,000 feet. The short-leaved pine (P. miti&j,
almost as valuable, is found in various parts, the quantity now
standing being estimated at 6,775,000,000 feet. The total value
of the pine timber of the State is about $250,000,000.
Agriculture is the leading industry in Mississippi. Over
300,000 of the population are directly engaged in the cultivation of
4,895,000 acres of land. The character of the soil ia varied, and
nil is productive, except that in the Flatwoods region and in the
district covered with long-leaved pine, where only the valleys are
fertile. At least half the State is exceptionally fertile. Not more
than one-fourth of the arable land has been brought into culti-
vation, and two millions of acres of the best lands in the State,
lying in the Bottom, might be made arable by proper drainage.
Cotton is the chief agricultural product ; m 1880 Mississippi
Bnked first among the States in the amonct raised. The crop of
1879-80 amounted to 955,808 bales, worth $43,000,000. There
wer^ produced also of cotton seed 28,000,000 bushels, worth
$3,000,000; of Indian com, 21,340,800 bushels; of oats, 1,959,620
bushels ; of wheat, 218,890 bushels ; of rice, 1,718,950 lb. Small
quantities of rye, barley, molasses, and tobacco, and abundant crops
of potatoes, yams, pease, and all garden vegetables, are annually
produced.
Fruits of various hinds flourish iu many parts of the Stale, and,
with early vegetables, are largely shipped to the northern markets
in spring and early summer. The value of the cotton crop is
about three times as great as that of all the other products of
the soil, which are sometimes insufficient for home consumption.
Economically this specialization of agriculture is to be regretted ;
but successful efforts are being made to diversify it by growing
other crops to which the soil and climate are equally well suitei
Manvfactiires. — The principal articles manufactured are lumber,
cotton and woollen goods, cotton seed oil, and agricultural imple-
ments.
Population. — The number of inhabitants according to the different
census returns from 1850 is given in the following table : —
Census.
Totcl.
While
Colooretl.
Density per
Sq. MUc.
1650
ISCO
1870
1880
C0S,626
829,609
1,131,692
295,718
353,910
384.649
479,371
310,808
437,404
445,060
652,221
13 09
17-07
1/-9
■2ii2
Of the coloured population, mostly freedmen and their descend-
ants, 1738 were Indians or half-breeds in 1880, and abont 60,000
mulattqes. The whites own nearly all the farms and other real
property. The total property valuation in the State decreased
from $607,324,911 in 1860 to $209,197,345 in 1870, on account of
the losses in war and the liberation of the slaves. There has been,
however, a rapid increase in the last decade. The towns in the
State have small populations : in 1880 Vicksburg had 11,814 in-
habitants, Natchez 7058, and Jackson, the State capital, 5204.
Administration., — The three departments, legislative, executive,
and judiciary, are similar to those of other States. The governor
and other executive officers are elected for four years. ' The legis-
lature, which meets biennially, is composed of forty senators,
serving four years, and one hundred and "twenty representatives,
serving two years. These are apportion.ed to the seventy-four
counties according to population, and elected by the people. The
judiciary officers, consisting of three justices of the supreme court,
twelve circuit judges, and twelve chancellors, are appointed by the
governor with the consent of the senate. One attorney-general
and twelve district attorneys are elected by the people. The State
maintains a public school system, with separate schools for the t^*0
races, costing in 18S0 $830,704, besides a State university and
other schools of high grade for each of the races.
History. — Mississippi was first visited by Europeans in 1540,
when the adventurous expedition of De Soto reached its northern
parts. After the disastrous termination of this expedition no
other Europeans visited this region nntU 1673, when Joliet and
Pfere Marquette descended the Mississippi to lat. 33°. In 1682 La
Salle and Tonty descended to the mouth of the river, and
claimed the whole region drained by it for the king of France,
giving it the name Louisiana. In 1699 the first colonists reached
the coast of Mississippi, sent from France under Iberville.
Settlements were made on Ship Island and Cat Island, and upon
the mainland on the eastern side of Biloxi Bay, at Bay St Louis,
and at Mobile. The colony did not prosper, and in 1712 Anthony
Crozat obtained by charter from the king all the commercial
privileges of the lower Mississippi valley, tfuder his management
the colony languished, and in 1717 the king accepted, the surrender
of his charter, and granted another with more extended privileges
to the "Western Company," or " Mississippi Scheme," with John
Law as director-general, and Bienville as governor of the colony.
Under this management the rich alluvial lands on the Mississippi
river began to be occupied ; tobacco, rice, and indigo were culti-
vated, and African slaves were introduced. Settlements were made
near the present city of Natchez in 1720. Two years later. Law's
company becoming bankrupt, much embarrassment in the colony
followed, and troubles also began with the natives. On November
28, 1729, the Natchez Indians surprised and murdered about 200
of the white male residents, and made captives of about BOO
women and children and negroes. A war followed, resulting in the
destruction of the Natchez tribe. The representatives of ^the
" Western Company " returned their franchises to the king in 1732,
the number of colonists and slaves being then about 7000. After
two unsuccessful campaigns against the Chickasaw Indians in the
northern part of what is now Mississippi, Bienville was superseded
by the Marqnis de Taudreuil in 1740.
By the treaty of Paris, in 1763, Franco ceded all her possessions
east of tlie lUssissippi river to England, excepting the island of
New Orleans, c^ded to Sp,rn, The British province of Weet
524
M I S — M I !S
Florida nt hrst I'xiended eastward from th« HissUsippi river slong
the Gulf coasts, with its noi'thern limit at the Slot pavillul of norlii
iatit.ude. Soon afterwards the northern boundary was fized at a
line drawn eastward from the point where the Yazoo river unites
^7ilh the Mississippi
Under British rule the Natchez country, whicn had been deserted
since the massacre of 1729, and the southern part of the present
State of Mississippi, rapidly filled with settlers, many of them
emigrants from the Atlantic colonies. Cotton, u-jTigo, and sugar
■were cultivated, and negro slaves continued to be freely introduced.
During the revolutionary war of the Atlantic colonies, "West
Florida, being far removed, remained undisturbed until 1779. Spain
and England being then at war, Galvez, the governor of New
Orleans, aided b}'' sympathizers with the revolutionary colonists,
took possession of tbe whole of West Florida for the king of Spain.
At the peace of 1783 England acknowledged the 3l3t parallel as
the southern bovmdary of the United States, and ceded West
Florida to Spain. The district between the 31st parallel and the
parallel through the mouth of the Yazoo was therefor^ claimed by
the United States and by Spain, the latter being in possession.
After tedious negotiations the latter power relinquished the district
in March 17S3, and Congress at once formed it into " the Mississippi
Territory," which extended from the Mississippi river eastward
■between the two above-mentioned narallels of latitude to the
Chattcihoochee riyer.
The State of Georgia claimed as a part of its domain all of the
district east of the Mississippi river, and between the 31st and S5th
parallels. In 1802 it ceded its claims to the Federal Government
for certain considerations, and in 1804 Congress extended the
limits of the Mississippi Territory northward to the 35th parallel.
^J" early all of the Territory was then owned by the native Indians.
The Choctaws occupied the southern part, and the Chickasaws the
northern part of what is now the State of Mississippi. In 1812
the United States troops occupied Spanish West Florida, and the
district east of Pearl river and south of lat. 31° was added to the
Mississippi Territory. The Territoi-y was divided by the present
line between Alabama and Mississippi, and the State of Mississippi
admitted into the Union in 1817. In 1830-32 the native tribes
exchanged their lands for others west of the Mississippi river and
were nearly all removed, and a rapid influx of settlers followed.
In January 1^61 the State seceded from the Federal Union, and,
ioining the Southern Confederacy, furnished a large number of
troops during the civil war. It was the field of many important
campaigns, and sulfered great losses. Exhausted by the conflict,
and harassed by procesies of political reconstruction, the State was
in a deplorable condition for several years. But within the lost
decade an era of prosperity commenced, marked by a large increase
in population and great activity in agricultural and other pursuits.
Literature. — Gayarrtf, History o/ Louisiana ; Monette, History of the Valley oj
the Mississippi. New York, lfi46 ; Claibomo, Mississippi as a Province, Territoi-y,
and State, Jackson, 1830; Wailes, Agriculture and Oeoloffy of Mississippi, J&ckaoa,
1854; Hilgard, Agriculture and Geolcgy of Mississippi, Jacksoii, 1860; Smith,
Outline of the Geology of Alabama, Montgomery, 1880; Wall, Handbook of Mis-
'issippi, Jackson, 1882. (R. E. F.)
MISSOLONGHI, or Mesolonghi (Meo-oXoyyioi'), a city
of Greece, the chief town of the nomarchy of Acarnania
and jEtolia, situated on the north side of the Gulf of
Patras, about 7 miles from the coast, in the midst of a
shallow lagoon, with a population of 6324 in 1879, is
notable for the siege of two months which Mavrocordatos
■with a handful of men sustained in 1821 against a Turkish
army 11,000 strong, and for the more famous defence of
1825-26 (see vol. xi. p. 125;. Byron died there in 1824,
and is commemorated by a cenotaph.
•jVli. MISSOURI, a Central State of the American Union,
lying almost midway between the Atlantic and the Rocky
Mountains, British America and the Gulf of Mexico. Its
eastern boundary is the Mississippi, separating it from
Illinois, Kentucky, and Tennessee. North and south its
boundaries ■with Iowa and Arkansas respectively are
mainly coincident with the parallels of 40° 30' and 36° 30'
N. lat.; but a small peninsula bet-ween the Mississippi
and St Fran5ois rivers stretches 34 miles farther south
between Arkansas and Tennessee. The western border,
■with Nebraska, Kansas, and the Indian Territory, is
nearly coincident ■with the course of the Missouri to the
junction of that stream with the Kansas, and then follows
the meridian of 17° 40' W. of Washington (94° 43' W.
of Greenwich). The area of the State is 65,350 square
miles, the extreme length from north to south 232 miles,
the extreme vndth 348 miles. Missouri is di^vided into
a northern and sourjc-m portion by the Missouri river,
flowing 400 miles in a generally easterly direction from
its junction with the Kansas to the point 12 miles above
St Louis where it unites ■with the MississippL Northern
Missouri has a surface broken and hilly, but not moun-
taiuouB. It is mainly prairie land, well watered by streams,
and fit for agriculture ; but there is a good deal of tiinber
in the ea.stera parts, especially along the bold blufls of the
two great rivers. Southern Missouri is almost equally
divided betT^een timber land in the east and prairie in
the west. In its south-western portion rises the table-land
of the Ozark hills (highest point 1600 feet above the sea).
The Osige, the Gasconade, and other streams flov? north-
ward and eastward into the Missouri. The south-eastern
lowlands form an undulating country, readily drained after
rain, ■with fertile ridges generally running north and south,
occasional abrupt isolated hills, forests of oak, hickory,
elm, maple, ash, locust, willow, persimmon, pecan, chestnut,
and cherry trees, and in the lowest parts swamps and
morasses. High rocky bluffs extend along the banks of
the Mississippi from the mouth of the Meramec river to
Ste Gsne^vieve, rising sometimes precipitously tO' the
height of 350 feet above the water, and low bottom lands
■with many lakes and lagoons extend from Ste Gene^vievo
to the AJkansas border. The south-east comer of the
State-is 275 feet above the sea, the north-east comer 445
feet, and the north-west comer 1000 feet.
Climate. — The climate of Missouri, lying as it does far
from the ocean ar.d unprotected by mountain ranges, ia
one of extremes in heat and cold, moisture and drought.
The Ozark range is high enough to influence the climate
locally, but not to affect that of the whole State. The
mean summer temperature for the ten years 1870-80
ranged from 75° in the north-west of the State to 78''"5 in
the south-east ; but the thermometer has been kno^wn to rise
to 104°. The winter- temperature averaged 33°'87 for
the whole State, varying from 28°'5 ia the north-west to
39°'5 in the south-east. In some winters the temperature
hardly falls to zero ; in others 20° below zero have been
registered. The Mississippi at St Louis freezes over once
in four or five years ; but this is partly caused by the
accumulations of floating ice coming down from the north.
The river has closed as early as the first week in December,
and, again, has remained open until the last week ia
Febraary. It is in cold seasons sometimes passable for
the hea^viest teams. The Missouri river is often closed
during the whole winter. The mean annual temperature
of the State varies from 53° to 58°. The climate is, on
the whole, dry ; for, in spite of the abundant rains, especi-
ally in the spring, evaporation is so rapid that the atmo-
sphere is rarely overloaded with moisture. April is the
driest month. The greatest amount of rain falls in the
south-eastern part of the State. An tmusual amount of
fair weather, prevailing clearness of sky, general salubrity
of soil and climate, are chief among the natural advantages
of this great State.
Geology. — The stratified rocks of Missouri belong to the
foUo^wing divisions : — Quatemaiy, Tertiary, Carboniferous,
Devonian, Silurian, and Arch^ai. The Quaternary system
comprises the drift, 155 feet thick ; the bluff, 200 feet above
the drift ; then the bottom prairie, 3-3 feet thick ; and on
the surface the alluvium, 3C feet in thickness. Claya ■with
strata of sands, marls, and humus form the alluvial bottomr;
of the two great rivers of the State, and make up a soil deep,
light, and incomparably rich. Beneath the alluvium is founci
the bottom prairie, made up also of sands, clays, and vege-
table moulds. This formation is found only in the bottom
lands of the Missouri and Mississippi rivers, and motr-
abundantly in those of the former. Numerous and weP-
presorvcd organic remains are foimd in the bottom prabie,
o Omaha
Ilttniiion^;^
MISSOURI
525
(ncludiog the shells found in great quantities in tne bluff
md remains of the mastodon and many trees and plants.
Bolow this formation, resting .upon the drift, is the bluff,
'fhis rests upon the ridges and river blufis, and thus is
vopographicaJly higher, although geologically lower, than
the bottom prairie. It is composed chiefly of a grey
siliceous marl, coloured sometimes to a deep brown or red
by the stains of oxide of iron. This formation extends
along the blufis of the Missouri from Fort Union to its
mouth, and is found capping those of the Mississippi from
Dubuque to the mouth of && Ohio. It is sometimes 200
feettluck; at St Joseph it is 140, at Booneville 100, at
St Louis 50, in Marion county only 30 feet. This forma-
tion has interesting fossils (Elephas primigeniusi &c.). The
drift, the lowest of the Quatemajy system, appears in the
altered drift, the boulder formation, made up largely of the
igneous and metamorphic rocks, with rocks from the Palaeozoic
strata upon which the others rest. Large boulders, five or
six feet in diameter, are found, usually of granite or metar
morphic sandstone ; no fossils except a few logs in the altered
drift have been found in this formation. The Tertiary
formation in Missouri is composed of clays, shales, iron
<>res, sandstone, and sand, and extends along the bluffs and
i>ottoins of the south-east part of the State. Iron ore is
found in this formation in great abundance ; sand of the
best quality for glass-making and clays for pottery and
stoneware also abound. Below the Tertiary bed are found
rocks which strongly resemble Cretaceous beds found in
other places in the United States. These strata are in such
a state of irregularity and disturbance as to indicate the
occurrence of some great movements after their deposition
and before the formation of the Tertiary strata. The Upper
Carboniferous system, or coal measures, made up of sand-
stone, limestone, marl, coal, and iron ores, covers an area
of more than 23,000 square miles in Missouri, occupying
the western and northern portions of the State. The supply
of bituminous and cannel coals found here would seem to
be well-nigh inexhaustible. In the Lower Carboniferous
rock are found many varieties of limestone and sandstone.
Among these are the Upper Archimedes Limestone, 200
feet; Ferruginous Sandstone, 3 95 feet ; Middle Archimedes
Limestone, 50 feet ; St Louis Limestone, 250 feet. The
Devonian system \s represented by limestone in Marion,
Balls, Pike, Callaway, Saline, and Ste Genevieve counties,
among which occtir the Chouteau ' Limestone, 85 feet ;
Lithographic Limestone, 125 feet; Onondaga Limestone,
100 feet. Of the Upper Silurian series are the following ,
formations: — Lower Helderberg, 350 feet; Niagara Group,
200 feet; Cape Girardeau Limestone, 60 feet. Prominent
among the Lower Silurian formations are the Trenton
Limestone, 360 feet ; the Black River and Bird's Eye
Limestone ; and the Magnesian series. The last-named
series is valuable both in a scientific and an economic sense.
It covers much of the southern and south-eastern portions
of the State, and in it are found vast deposits of lead,
zinc, copper, cobalt, iron ores, and marble. The Archaean
rocks occur below the Silurian deposits, and contain siliceous
and other slates in which no fossils are found. The porphyry
rocks of this formation also contain iron ores.
QxU. — The exposed coal in Missouri includes upper, middle, and
lower measures. In the first are about i feet of coal, and the area
of exposure is about 8400 squara miles. The middle coal measures
contain about 7 feet ol coal, and cover an exposed area of about
2000^ square miles.* Hie lower measures have fivs workable seams,
varying from 18 inches in thickness to 4j fe«t, and also some thin
seams- of only a few inches. In 1880 666,304 bushels of bitu-
minous coal were raised in thirty-five counties of Missouri, the
value at the pit mouth being $1,060,225. $642,772 were paid in
wages to 2599 persons. The Missouri coal mines are easHy worked.
/nm. — The iron ores are red haanutite, red oxide, specular iron,
brown hematite or limonite, and clay ironstone. Manganiferous and
sSicaoua specular ores occur in the porphyries of the Aichaan rocks,
and in trie gniuites. The greatest exposure of specular iron yet dis-
covered is Iron Mountain, the purest mass or body of irpn ore Known.
Analysis shows it to contain from 66 to 69 per cent, of metallic iron.
The ore of Shepherd Mountain is not so rich as that of Iron Moun-
tain, but is uniform in character, free from sulphur and phosphoric
acid and on the whole superior to any other yet developed in Missouri.
Pilot Knob ore gives 53 to 60 per cent, metallic iron, and has few
deleterious substances. It is fine-grained, light bluish grey in
colour. The ore of the Scotia iron banks and Iron Ridge are much
alike in appearance and character, being specular boulders imbedded
in soft red luematite. In some of these boulders are cavities in
which the ore has taken botryoidal form, and upon these peroxide of
iron crystallizations are so formed that a gorgeous show of prismatic
colours is presented. The above are the chief deposits of iron ores,
but limonites are found mostly in the southern parts of the State.
The counties of Ste Geneviere, Madison, St Frani;ois, Cape Girar-
deau, Bollinger, Wayne, Stoddard, ■Washington, Reynolds, Shan-
non, Carter, and Kipley have the greatest exposures of these ores,
although they are found in many others. The supply of iron ores
is, indeed, practically inexhaustible.
Lead. — Second only to iron among the metals of Missouri is the
vast deposit of lead found in the southern parts of the State. The
great disseminated lead region occupies about one-half of the noi'ch-
em portion of Madison, and about as much of- St Fran9oi3 coxmty.
It is in the magnesian limestone that the largest (quantities have
been found. In Franklin county galena is found in abundance in
ferruginous clay and coarse graveL In the great mammoth mine
in 'Washington county is a succession of caves in which nullions oi
pounds of lead were found adhering to the sides and roofs. The
central lead district of the State comprises the counties of Cole,
Cooper, Moniteau, Morgan, Miller, Benton, Maries, Camden, and
Osage ; the southern lead region the counties of Pulaski, Laclede,
Texas, "Wright, Webster, Douglass, Ozark, and Christian. The
"western lead district includes the counties of Hickory, Dallas, Polk,
St Clair, Cedar, and Dade ; the south-western the counties ol
Jasper, Newton,. Lawrence, Stone, Barry, and M 'Donald. The
two counties Jasper and Newton produce fully one-half of the pig
lead of Missouri. The lead mines of Granby are - among the best-
known" in the State, and millions of pounds of lead have been taken
from these lands.
Copper deposits have been found in several counties, ohiefiy ia
the south-western part of the State. Zinc is found, in the shape ol
sulphuret and also silicate of zinc, in nearly all the lead mines in
south-western Missouri. It has often occurred in such masses 'a£
seriously to hinder mining operations, and until very recent years,
when railroad facilities have given this ore a market, it was thrown
aside as worthless. It is now an important and profitable adjunct
of the lead mines of Missouri. Cobalt and nickel are found at Mine
La Motte and in a few other places. . Silver is found in small quan-
tities in lead mines in Madison county, combined with the lead.
Clays for the manufacture of ordinary brick for building purposes
and for fire-brick exist in quantities 'beyond computation, and
kaolin has been found in a few places. Marble of various shades
and qualities abounds in Missouri, and is an important item in its
mineral wealth. Limesfimes and sandstones suitable for building
purposes are found in many parts of the State.
Agriculture. — Indian com, wheat, oats, and tobacco are the staple
products ; but cotton, hemp, and flax are also raised to some extent
in the southern counties. The average yield of wheat to the acre
is 30 bushels, and that return is often far exceeded. No flour is
of a higher quality or more in demand in foreign as well as home
markets than that made from Missouri wheat. Indian com is
especially used in fattening live stock. Blue grass, timothy, red-top,
and red and white clover grow luxuriantly, and favour stock-raising.
In some parts of the State pasturage can be had all the year round,
and the cheapness of com makes the raising of pork, in particular,
a very profitable business. All varieties of fruit can be very suc-
cessfidly cultivated. , The more tender fruits, such as apricots, nec'
tarines, figs, and many choice kinds of grapes, grow here as well as
the more northern fruits — the apple, the pear, the plum, and the
cherry. Apples and peaches do well in all parts of the State. Sii
native varieties of grapes are found in luxuriant growth, and many
cultivated varieties have ■ been successfully introduced. No State,
not even California, can hope ultimately to rival Missouri in the
production of both red and white wines. Sheep-raising has proved
remunerative in flie southern counties chiefly, where the mild cli-
mate, the fine grasses, and the abundance of good water are especially
favourable to this branch of agricultural mdustry. There are in
Missouri, in round numbers, 10,000,000 acres of improved and
13,000,000 of unimproved land, including 9,000,000 acres of wood-
land. The cash value of the farms is estimated at $90,000,000.
In 1880 there were on the farms in the State 667,776 horses,
192,027 mules and asses, 9020 oxen, 661,405 cows, 1,410,507 other
cattle, 1,411,293 sheep, and 4,653,123 swine. Missouri is the fourth
maize-produciug State of the Union ; it supplies more wine than
any State except California, and is a rival of Kentucky, "Virginia,
Tennessee, and Maryland in the culture of tobacco, which is a
526
MISSOUEI
staple in the rich counties in the northern central part of the
State, bordering upon the Missouri river. No State raises so
many mules, asses, and hogs. The production of cereals in 1880
was— corn, 202,485,723 bushels ; wheat, 24,966,627 bushels ; rye,
535,426 bushels ; oats, 20,o70,958 bushels ; barley, 123,031 bushels ;
buckwheat, 67,64;0 bushels. The production of tobacco for the same
year was 12,015,657 lb from 15,521 acres, valued at 3600,256.
Three -fouiths of this amount was raised in Chariton, Marion,
Randolph, Howai-d, Callaway, and Saline counties.
fFild Animals. — Red-deer are found in every part of the State,
espficially in the thinly -settled and mountainous districts. Venison,
indeed, in its season, is as cheap as good beef in the markets of St
Louis. Wild turkeys are numerous in the swampy and mountainous
districts, and are found in all parts of the State. Prairie chickens,
or puinated grouse, are found in the prairie portion of Missouri, and
are shipped in great numbers to Eastern markets. In all parts of
ilissouii are found the quail or Virginia partridge, thousands of
ban-els of v/hich are shipped from the State each season. The
rabbit, a species of hare, is so common as to be considered a pest.
The grey squirrel and the red fox-squirrel are also found in lar^e
numbers all over the State. Black bass, perch, catfish, buffalo
fish, suckers, and pike are the leading varieties of native fish..
Manufactures. ~lu 1880 Missouri had about 20,000 manufactur-
ing establishments, in which a capital of about $125,000,000 was
employed. The products of these establishments were valued at
upwards of $300,000,000. The leading manufacturing counties
cutside of the city of St Louis are Jackson, Buchanan, St Charles,
ilarion, Franklin, Greene, Cape Girardeau, Platte, Boone, and
Lafayette ; but more than three-fourths of the manufactures are
produced at St Louis, which is the fourth manufacturing city of
the Union. The chief manufacture is that of flour, wMcli employs
about 900 mills, and is rapidly increasing. Twenty-four mills made
ia St Louis, in 1880, 2,142,949 barrels of flour, having a daily out-
put of more than 11,000 barrels. St Louis millers and dealers
sent in 1880 to Europe and South America 619,103 barrels of flour ;
and at the world's fairs at Paris, Vienna, and Philadelphia, Missouri
flour received the first award. The iron industry, which stands second
in importance, is yet only in its infancy, and St Louis seems destined
to be one of the great centres of iron and steel manufacture. The
amount of iron made in Missouri in 1880, in twenty-two establish-
ments employing 3139 hands, was 125,758 tons. St Louis made the
.^a;no year 1 02, 664 tons of pig-iron, steel, and rolled iron and blooms.
Th2 yearly values of a number of other industries are estimated as
Toilows :— meat packing, $20,000,000 ; lumber, $10,000,000 ; bags
and bagging, $7,000,000; saddlery, $7,000,000; oil, $6,000,000;
printing and publishing, $5,500,000; furniture, $5,000,000; car-
riages and waggons, $4,500,000; marble and stone, $4,000,000 ;
tin, copper, and sheet-iron, $4,000,000; agricultural implements,
$2,000,000. The manufacture of glass and glass-ware is carried on
to a considerable extent, especially in St Louis. At Crystal City,
on the Mississippi, 30 miles below St Louis, is a very large
deposit 0? sand- suitable for the manufacture of plate-glass, and a
company has been organized and is now in successful operation,
with a capital of $1,000,000.
Commerce. — The extensive commerce of Missouri centres at St
Louis, bebveen which city and the ports on the Mississippi and
Missouri rivers steambo^its are constantly plying. Railroaa trans-
portation has, in recent years, furnished superior and cheaper
tacilities for much of the ti'ade which fonnerly depended upon the
rivers. The trade in cotton especially has been greatly increased
in Missouri since 1870 by the use of railroad transportation, which
has made St Louis one of the great cotton centres of the United
States. Extensile cotton presses were built in St Louis in that
year, and the receipts of cotton from the more southern States has
increased rapidly — from 12,264 bales in 1869-70 to 457,563 bales in
1879-80. Railroad connexions have made the interior portions
of Arkansas and Texas more accessible to St Louis than to the
southern ports of shipment, and the trade ■n*ith the south-west,
with the Indians, and with llexJco is constantly increasing. In 1870
St Louis was made by Act of Congress a port of entry to which
foreign merchandise could be brought in bond. The value of the
direct imports for the year ending 30th June 1882 was $1,934,342.
Population. — Missouri is divided into 114 counties. The following
table gives the number of inhabitants since 1850 : —
Tear.
lUles.
Females.
Total.
Density per
square mile.
1850
1860
1870
1880
357,832
622,201
896,847
1,127,187
321,212
559,811
824,948
1,041,193
682,044
1,182,012
1,721,295
2,108,380
14-37
18 03
26-34
31-55
In 1880 the foreigu-'born residents numbered 211,678, or 9-7 per
cent, of whom 109,974 wero Germans and Scandinavians; tlioro
wore also 145,046 of African descent. The early settlers of the State
■were French, and their descendants are still found in St Loub and
Sto Genevieve and a few other smaller to^vns. Many Germans have
recently settled in all parts of the State, while English, Irish, Scotch,
and Swedes have also made Missouri their home in considerable
numbers. The native American population is mostly descended
from immigrants from the States of Kentucky, Tennessee, North
Carolina, and Virginia. During recent years there has been a large
accession to the population from the eastern and north-western
States.
St Louis, the chief city of the Mississippi valley, situated
upon the Mississippi river about 12 miles below the month of the
Missouri, has a population of 350,618 ; Kansas City, a thri-.-ing
town on the western border, situated on the banks of the Missouri,
has 56,785 ; St Joseph, in ths north-west, has 32,431 ; Hannibal,
in the north-east, has 11,074 ; and Jefferson City (the State capital),
in the centre, has 6271.
Education. — Missouri has a public school system of education
first adopted in 1839. There are district schools, elementary and
ungraded ; city schools, graded, with high school courses ; four
normal schools, and a State university. Free public schools for
white and coloured children between the ages of six and twenty
years are required by law for every district in the State. Besides
these public institutions supported by the State there are many
private schools and colleges for both sexes. Chief among these are
the St Louis University, an institution managed by the Jesuits ;
the College of Christian Brothers, also under the control of the
Roman Catholics ; and Washington University, a non-sectarian en-
dowed school, which has property estimated at §1,000,000, and
more than 1300 students. The Baptists have a college at Liberty
called William Jewell College ; the Congregationalists one at Spring-
field called Drury College ; and flie Methodists and Presbyteriaiu
several colleges and seminaries.
Eeligion. — The early settlers of Missouri were Roman Catholics,
and in the river towns may be found to-day a large number of that
faith. The Baptists have 88,999 members, with 1385 churches ;
the Methodists, 95,270 members and 918 churches ; the Protestant
Episcopal Church, 25,000 members and 65 church buildings ; the
Presbyterians, with their various branches, 34,628 members and 706
chui'ches.
Administration. — The lerislativo power is vested in a body con-
sisting of a senate and a house of representatives, which meets
once in every two years, on the "Wednesday after the first day of
January next after the election of the members thereof Members
of the legislature .are paid a sum not to exceed S5 a day for th»
first seventy days of the session, and after that not to exceed $1 a
day for the remainder of the session. They are also allowed mile-
age. The executive department consists of a governor, a lien-
tenant-governor, a secretary of state, a State auditor. State
treasurer, an attorney-general, and a superintendent of public
instruction ; these are all elected by the people. The supreme
executive power is vested in the governor, who is chosen for four
years, as also aro the other members of this department. The
governor has a qualified veto upon the acts of the legislature, and
such other powers as are common to that officer in the several
States. The judicial power of the State is lodged in a supremo
court, the St Louis court of appeals, circuit courts, criminal
courts, probate courts, and municipal courts. All judicial officers
are elected by the people. Judges of the supreme court are elcct«l
for ten years, those of the St Louis court of appeals for twelvs
years, those of the circuit courts for six years. Executive and
judicial officers are liable to impeachment by the house of repre-
sentatives. All impeachment cases are tried by the senate.
Every male citizen of the United States, and every male pcrso«
of foreign birth who may have declared his intention to become a
citizen of the United States, according to law, not less than one
year nor more than five years before he offers to vote, who is over
the ago of twentj'-one years, is entitled to voto at all elections by
the people, if ho has resided in the State one year immediately
preceding the election at which ho offers to vote, and has resided
iu the county, city, or town where ho shall offer to voto at least
sixty davs immediately preceding the election.
History— 0-:i the 9th April 1682, the French voyager and dis-
coverer La Salle took possession of the country of Louisiana in the
name of tho king of Franco. Its limits wore quite indefinite, and in-
cluded the present territory of Missouri (see Louisiana). The first
settlements of Missouri wore made in Sto Genevieve and at Kew
Bourbon, but uncertainty exists as to the exact date. By soma
the year is fixed at 1763 ; by others, and by many traditions, as
c.arly as 1735. St Louis was settled by Pierre Laclede Liguest, a
native of France. Tho site w.as chosen in 1763, and in February
17C4 Augusto Chouteau went at tho order of Liguest to the spot
previously selected, and built a small village. For a long tini«
the settlements wero confined to the neighbourhood of the river.
On the Slst of October 1803 tho Congress of the United States
passed, ah Act by which the president vi-as authorized to taJM
pos-icssicn of the tenitory according to the treaty of Pajis, and tho
formal transfer of Lower Louisiana was made on 20th Decembcc
M I S — M I T
627
loC3. In 1801 Co'igrcsi diTidcd the territory into two portions.
The northern part, conunonly called Uppar Louisiana, was taken
possession of in March 1804. In June 1812 Missouri waa organ-
ued as a Territory, with a governor and general assembly. The
first governor (1813-1820) was 'Williain Clarke. hi 1818
Mlssonri applied for admission to the Union as a State. Two
years of bitter controversy followed, which convulsed the country
and threatened the dissolution of the Union. This controversy
followed a resolution introduced into Congress which had in view
an anti-slavery restriction upon the admission of Missouri to the
Union. This was at last settled by the adoption of the " Missouri
compromise," which forbade slavery in all that portion of the Louisi-
ana purchase lying north of 36° 30" except in Missouri, and on
19th July 1820 ilissouri was admitted to the Union. A conven-
tion to frame a constitution had ali'eady been called, and the
constitution then adopted remained without material change until
1865. The first general assembly under the constitution met in
St Louis in September 1820, and Alexander M'Nair was chosen
governor in August. The seat of government was fixed at St
Charles in 1820, and removed to Jeferson City, the present State
capital, in 1826. The first census of the State was taken in 1821,
when the number of inhabitants was found to be 70,647, of whom
11,254 were slaves. In the Black Hawk war in 18S2, the Florida
war in 1837, and the Mexican war in 1846 Missouri, volunteer
troops did their share of the work. In the troubles in Kansas, and
the bitter discussion upon the question of slavery, Missouri was
deeply involved, A strong feeling in favour of secession showed
itself in many parts of the State. Governor Jackson, in Ms
inaugural address on the 4th of January 1861, said that Missouri
must stand by the slaveholding States, whatever might be their
course. The election of a majority of Union men, however, as
delegates to a convention called to consider the affairs of the
nation,, showed that public sentiment was hostile to secession, and
the convention adjourned \rithout committing the State to the
secession party. United States troops were soon gathered at St
Louis, and forces were also sent to Jefferson City, and to Rolla.
Governor Jackson fled from the capital, and summoned aU the
State troops to meet him at Booneville. General Lyon defeated
these troops, 17th June 1861, and soon most of the State was
under the control of the United States forces. The State conven-
tion was reassembled. This body declared vacant the offices of
governor, lieutenant-governor, and secretary of state, and filled
mem by appointment. The seats of the members of the legislature
wore also declared vacant. Governor Jackson soon issued a pro-
clamation declaring the State 'out of the Union, and Confederate
forces wefb assembled in large numbers in the south-western part
of the State. General Lyon was killed at the battle of Wilson's
Creek near Springfield, and General Fremont, commanding tho
department of the west, decreed martial law throughout the State.
For a year matters were favourable to the Confederates, and at the
opening of 1862 their troops held nearly half the State ; but in
February a Federal force under General Curtis drove General Price
into Arkansas. He returned in 1864, and overran a largo part of
the State, but was finally forced to reticat, and but little further
trouble arose in Missouri during the war. Missouri furnished to
the United States army during the war 108,773 troops. In 1865
a new constitution was adopted by the people. In 1869 the XT.
Amendment to the United States constitution was adopted by a large
majority. In 1875 still another State constitution was drawn up
by a convention called for that purpose, and ratified by the people,
and is now the fundamental law of he State. (M. S. S.)
MISTLETOE ' (Viscum album, L.), a species of Viscum,
of the family Loranthacese. The whole genus ia parasitical,
and seventy-six species have been described ; but only the
mistletoe proper is a native of Europe. It forios an ever-
green bush, about 4 feet in length, thickly crowded with
(falsely) dichotomous branches and opposite leaves. The
leaves are about 2 inches long, obovate-lanceolate, yellowish
gi-een ; the dioecious flowers, which are small and nearly
of the same colour but yellower, appear in February and
March ; the fruit, which when ripe is filled with a viscous
semltransparent pulp (whence birdlime ia derived), is
almost always white, but there is said to be a variety with
red fruit. The mistletoe is parasitic both on deciduous and
evergreen trees and shrubs, and " it would be difficult to
' Greek l^ia or i{(Jr, hence Latin viscum, Italian vischio or msco,
r.nd French gui. The English word is tho Anglo-Saxon misteltan,
Icelandic mistelteinn, in which tan or teinn means a twig, and mhtd
may be associated either with mist in the sense of fog, gloom, because
of the prominence of mistletoe in the dark season of the year, or with
the same root in tho sense of dung (from the character of the berries
or the supposed mode of propagation).
say on what dicofcyledonoui! trees it does not grow"
(Loudon). In England it is most abundant on the apple
tree, but rarely found on the oak. The fruit is eaten by
most frugivorou.^ birds, and through their agency, particu-
larly that of the thrush (hence, missel-thrush or mistle-
thrush), the plant is propagated^ (The Latin proverb has
it that "Turdua malum sibi cac3.t"; but the sowing ia
really efiected by the bird wiping its beak, to which the
seeds adhere, against the bark of tho tree on which it has
alighted.) The growth of the plant is slow, and its dura-
bility proportionately great, its death being determined
generally by that of the treo on which it has established
itself. See Loudon, Arboretum, et Fruiiceium Brkannicum,
vol iL p. 1021 (1838). The mistletoe so extensively used
in England at Christmas tide is largely derived from the
apple orchards of Normandy.
Pliny (H. N., xvi. 92-95; xxiv. 6) has a good deal to tell about
the viscum, a deadly parasite, though slower in its action than ivy.
He distinguishes three ''genera.'' **0n the fir and larch grows
what is called stclis in Euboea and hyphcar in Arcadia. " Viscumj
called dryos hyphcar^ is most plentiful on the esculent oak
(quercus), but occurs also on the robur, Prunus sylvestris, and
terebinth. Hyphear is useful for fattening cattle if they are hardy
enough to withstand the purgative effect it produces at first ;
viscum is medicinally of valne as an emollient, and in cases of
tumour, ulcers, and the like; and ho also notes it "coneeptum
fcemiuarum adjuvare si omnino secum habeant.'* Pliny is also our
authority for the i:everence in which the mistletoe when found
growing on the robur was held by the Druids. The robur, he says,
13 their sacred tree, and whatever is found growing upon it they
regard as sent from heaven and as the mark of a tree chosen by
Gwi Such cases of parasitism are rare, and when they occur
attract much attention (est autem id tarum admodum inventu et
repertum magna religione petitur), particularly on the sixth (day
of the) moon, with which tneir months and years and, after the
lapse of thirty years, their "agec " begin. Calling it in their own
language "all heal" (omnia sanantem), after their sacrifices and
banquets have been duly prepared under the tree, they bi-ing near
two white bulls whose horns are then for the first time bound.
The priest clothed with a white robe ascends the ti'ee, cuts [the
mistletoe] with a golden hook; it is caught in a white mantle.
They then slay the victims, praying God to prosper His gift to them
unto whom He has given it. Prepared as a draught, it is used as a
cure for sterility ana a remedy for poisons. The mistletoe figures
also in Scandinavian legend as having furnished the material of
the arrow with which Baldur (the sun-god) was slain by the blind
god Hiider. Most probably this story had its origin in a particular
theory as to the meaning of the word mistletoe.
MITAU (the Lettish Jelgava), a town of Eussia, capital
of the government of Courland. It is situated 27 miles
by rai). to the south-west of Riga, on the right bank of tho
river Aa, in a fertUe plain which rises only 12 feet above
sea-levsl, and which probably has given its name to the tow;i
(Mitts in der Aue). At high water the plain and sometimes
also the town are inundated. Mitau is surrounded by a
canal occupying the place of former fortifications. Another
canal waa dug through the town to provide it vrith water;
but this now receives the sewage, and water is brought in
cars from a distance of S miles. Though so near Riga,
Mitau has quite a difEerenc character. It has regular
broad streets, bordered with the lovr pretty mansions of
the German nobility who reside at the capital of Courland
either to enjoy the social amusements for which Mitau is
renowned or to provide education to their children. Mitau
is well provided with educational institutions. A gym-
nasium occupies a former palace of the dukes of Courland,
and has a rich library; and there are about forty other
schools. The town is also the seat of a society of art and
literature, of a natural history society, which has a good
local museum, and of tho Lettish Literary Society. The old
castle of the dukes of Courland, which has witnessed so
many conflicts, was destroyed by the Duke Bu-on, who
erected in its place a spacious palace, now occupied by the
governor and the courts. Mitau has 22,200 inhabitants,
mainly Gfermans, but including also Jews (about COCO),
Letts (5000), and Russians. Manufactures are few, those
528
I T
of wrouglit-iron ware and of white-lead being the most im-
portant. • The river Aa brings Mitau in connexion with the
trade of Riga, small vessels carrying goods to the amount
of about £150,000 a year.
Mitau is supposed to have been founded in 1266 by the grand-
master Conrad Slandern. It has often changed its rulers.' In
1345, when it was plundered by Lithuanians, it was aheady an
important town. In 1561 it became the residence of the dukes of
Oourland. During the 17th century it was thrice taken by the
Swedes. Russia annexed it with Courland in 1795. At the be-
^ning of this century it was the residence of the count of
Provence (afterwards Louis XVIII.). In 1812 it was taken by
Napoleon I.
MITCHEL, Ormsby M'Knight (1810-1862), American
general and writer on astronomy, was born in Union county,
Kentucky, August 23, 1810. He began life aa a clerk,
but, obtaining an appointment to a cadetship at West Point
in 1825, he graduated there in 1829, and became assistant
professor of mathematics in 1831. Subsequently he was
called to the bar, but forsook law to become professor of
mathematics and natural philosophy at Cincinnati college.
There he established an observatory, of which he became
director. From 1859 to 1861 he was director of the
Dudley observatory at Albany. He took part in the war
as brigadier-general of volunteers, and for his skill and
rapidity in seizing certain important strategic points was
on April 11,.1862, made major-general. He died of yellow
fever at Beaufort, South Carolina, October 30, 1862.
Besides making important improvements on several astrono-
mical instruments, Mitchel was the author of several works
on astronomy, the principal of which are The Planetary
and Stellar Worlds (1848) and The Orbs of Heaven (1851).
See Memoir by Headley (1865).
MITCHELL, Sir Thomas Livingstone (1792-1855),
Australian explorer, was a son of Mitchell of Craigend,
Stirlingshire, where he was born, June 16, 1792. From
1808 to the end of the Peninsular War he served in
Wellington's army, and for his services received the medal
and five clasps, and was raised to the rank of m.ajor. He
was appointed to sui-vey the battlefields of the Peninsula,
and his map of the Lower Pyrenees is still admired. In
1827 he was appointed deputy surveyor-general, and after-
wards surveyor-general, of New South Wales. He devoted
himself to the exploration of Australia, making four
expeditions for that purpose between 1831 and 1846.
During these expeditions he discovered the Peel, the
Namoi,. the Gwyder, and other rivers, traced the course
of the Darling and Glenelg, and was the first to pene-
trate into that portion of the country which he named
Australia Felix. His last expedition was mainly devoted
to the discovery of a' route between Sydney and the Gulf
of Carpentaria, and during the journey he explored the
Fitzroy Downs, and discovered the Balonne, Victoria,
Warrego, and other streams. In 1838, while in England,
Mitchell published the narrative of his first three journeys,
Three Expeditions into the Interior of East Australia (2
vols.). In 1839 he was knighted and made a D.O.L. of
Oxford. During this visit he took with him some of the
first specimens of gold and the first diamond found in the
country. In 1848 the narrative of his second expedition
was pubKshed in London, Journal of an Expedition into
the Interior of Tropical Australia. In 1851 he was sent
to report on the Bathurst gold-fields, and in 1853 he again
visited England and patented his boomerang propeller ior
steamers. He died at his residence at Darling Point,
Sydney, October 5, 1855.
Besides the above works, Mitchell wrote a book on Geographical
end Militanj Surveying (1827), an Australian Ocography^ Slid a
translation of tlio Lusiad of Camoens.
MITE. Mites (Acarina) are minute creatures which
form a large division of the Arachnida, distinguished by
-MIT
the absence of any constriction between the cophalothcrax
and abdomen. Linucciis included all in the single geni;s
Acarus. They are now divided into several families (mostly
containing numerous genera),
viz., Trombidiids! (harvest ,
mites), usually scarlet specks '
seen running on stones, grass,
ic, in hot weather ; Teira-
nychi, which, although not
bright red, are the red spider
of our green-houses, and are
distinguished by feet with
knobbed hairs ; Bddlida:,
long-snouted mites with an-
tenniform palpi ; Ckeyletidm
(fig. 1), the so-called book
mites, — ferocious, predatory
little beings, quite uncon-
nected with books ; Hydrachnidx, freshwater mites with
swimming legs, mostly beautiful creatures of brilliant
colours; Limnocaridse, crawling freshwater or mud mites;
Halicarid^, chiefly marine ; Gamasidm, hard-skinned brown
mites often parasitic on insects, and best known by .the
females, and young of both sexes, found on the common
dung beetle (Oeotrupes stercorarius) ; Ixodidm, the tmo
ticks, not to be confounded with the sheep-tick, &c., whick
-CheyUius flabdli/er.
Fio. 2. — Leiosoma palmicinctum ; nympb.
are wingless flies ; Oribatidse, beetle mites, so called from
their resemblance to minute beetles (these are never
parasitic; they undergo transformations almost as strange
as those of insects, many of the immature forms being
quaint and beautiful, see fig. 2); Myobiadie, bizarre para-
sites of the mouse, &c., with peculiar holding claws ;
Tyroglypkidx, the cheese mites ; Analgids, found on the
feathers of birds ; Sarcoptid-m, the itch mites ; Arctisconidic,
the water bears ; Demodicidee, found in the sebaceous
follicles of the human nose, &c. ; and Phytoptidx, the gali
mites, which attack the leaves of plants, making tiny gall-
Uke excrescences.
The sexes are distinct individuals; the reproduction is
oviparous; the larva is almost always hexapod, though the
later stages have eight legs ; that answering to the pupa of
insects is active, and is called the nymph. The breathing
in the first-named eleven families is tracheal, the position of
the stigmata varjdng greatlj' ; in the last-named six families
it is by the general body surface. No heart or circulation of
the blood is known to exist ; the alimentary canal is usually
somewhat on the insect type, but with cKcal prolongations
to the stomach, the reproductive organs often more on the
crustacean type. There is generally a single very large
nerve-ganglion above the oesophagus, sending nerve-branches
to the various parts. The legs hr.ve ordinarily five to
I T— M I T
529
seven joints, rarely three; the feet are usnally terminated
by claws or suckers, or both, sometimes by bristles. Tue
mandibles are generally large, oftenest chelate (like a
lobsters claw), sometimes style-like piercing organs, and
of other forms. The maxilla: vary much: they may be
piercing or crushing organs, or may coalesce to form a
maxillary lip; there is ustiaUy one pair of maxillary palpi,
no others. Sometimes there is a lingua, and iu the
Gamasidx a galea. Antennae are not found.
Mites are distributed all over the known world. They
have been found in Franz-Josef's Land and Spitzbergen
and in the hottest tropical regions, as well as the temperate
zones. Often very similar .species come from all parts.
They are numerous in amber of the Tertiary epoch.
The best-known species are probably those which injure
man or his works, viz., the itch mite, the cheese mite, the
scM»Ued harvest-bug, and the red iipider. The dog-tick
is also well known.
The itch mite (Sarcoptet scabiei, fig. 3) is a minute, almost
circular, flattened, colourless creature, with skin covered
with wavy wrinkles, and a number of triangular points
arising from that of the back ; legs short, the two front
pairs and the fourth pair in the male terminated by suckers
on long stalks, the two hind
pairs in the female and third
pair in the male having long
bristles instead. It is parasitic
on human beings: the males
and young remain chiefly on
the surface of the skin, but
are difficult to find; the female
burrows under the scarf-skin,
causing the intense itching
of scabies by the action of
her chelate mandibles as she
eats her , way. A small
watery pustule is raised near
where the acarus has entered
the skin, and others arise ;
the creature is not found in F'«;.3;-Th'Ite''Mi'f (*«''i'.<"
»!. ^ 1 u X X iL f .1. 'cabiei) ; reniale. After Meguin.
the pustule, but at the further
end of a short tunnel which may be half an inch long. The
eggs are laid, in the tunnel after the acarus has passed;
they hatch and multiply rapidly. The disease can be
certainly cured ; the usual mode is to rub the whole body
with sulphur ointment, which is best done after a warm
bath, allow it to remain on all night, and wash off in the
morning. This treatment should be repeated once or twice
at intervals of a day or two. Other applications of sulphur,
as sulphijrons acid, sulphur vapour baths, <te., are efficacious.
All clothes which have touched the skin must be disinfected
by heat. The disease is highly contagious. Most mammals
have their peculiar varieties of itch mite.
The cheese mite (Tyroglyph-as siro) is an elliptical, fat-
bodied, colourless acarus with smooth skin and very long
hairs. It breeds iu thousands in old cheese, flour, grain, (fee,
and does much damage. There are numerous allied species ;
some belonging to the genus Glyciphagiis are elegantly
ornamented with plumes or leaf-like hairs.
The red-spider {Tetranyclms tdarius) attacks the leaves
of plants or trees, and is a great pest in green-houses. It
spins a slight web on the surface of the leaves, and lives in
companies on the web ; it is of a rusty red or brown.
The harvest bugs, thought by some ivritcrs to be a
species, and by them called Leptus antumiKiHf, are simply the
larvae of several species of Trombidium. They are prcdatorj-,
but will attach theni.-.elves temporarily to the human skin,
and produce the violent itching felt on the lower parts of
the legs after walldng through dry grass in autumn. On
inspection with a gl;..'!s the creature may be seen as a
■ li;— 20
minute scarlet point. A drop of beniiiie will prubably get
rid of the intruder.
The dog tick, like the harvest-Dug, is not rcaily parasitic
on mammals, though it attaches itself tempoiariiy; its
ordiriury food may ;)robably be vegetable. (a. d. m.)
MITFOED, Maev Russell (1786-1 855), born at Aires-
ford, Hampshire, on the IGth of December 1786, retains
an honourable place in English literature as the authore-s
of Our Tillage, a series of sketches of village scenes ani!
characters unsurpassed in their kind, and after half a
ceutu-TT of in'.itations as fre^h as if they had been writtci
yesterday. AVashington Irving was iliss Mitford's literary
model, but her work is thoroughly original and spontaneous,
the free outflow of a singularly charming character. The
shortest account of her life would be incomplete without a
reference to the scapegrace father who was the centre of
her affections, and the " only begetter " of all that is most
delightful and characteristic in her writing. Dr Slitford
first spent his wife's fortune in a few years; then he spent
also in a few years the greater part of £20,000 which his
daughter drew (in 1797, at the age of ten) as a prize in a
lottery; then he lived, for most years of his life, on a
small remnant of his fortune and the proceeds of his
daughter's literary industry. In the little village of Thi-ee
MOe Cross, near Reading, in a small cottage which Jliss
Mitford says was "a fine lesson in condensation," ihi
doctor was the stay, support, and admiration of all the
loafers in the neighbourhood, while his daughter, who had
called herself his mamma, and treated him as her little coy
from the time when she was herself a little girl, found ai(
unfailing charm in his "friskings," and was the loving
slave of all his good-humoured exactions. The father kept
fresh in his daughter the keen delight iu incongruities,
the lively sympathy with self-willed vigorous individuality,
and the womanly tolerance of its excess which inspire sc
many of her sketches of character. The woman who lived
in close attendance on such an " awful dad," refused all
holiday invitations because he could not live without her;
and worked incessantly for him, except when she broke oS
her work to read him the sporting newspapers, evidently
wrote from the heart in her bright portraits of such
characters as the Talking Lady, the Talking Gentleman,
Joel Brent, Jack Rppley, Tom Cordery, Lizzy, Lucy, and
Harriet. Her writing has all the charm of perfectly
unaffected spontaneous humour, combined with quick wit
and exquisite literary skill. She died January 10, 1855.
Miss Mitford's youthful ambition was to bo " the gicatest English
poetess," and her first publications were jwems in the manner of
Coleridge and Scott {Miscellaneous Verses, 1810, of sufficient mark
to be reviewed by Scott iu the QimrUrly ; Christine, a metrical tale,
1811 ; Blanche, 1813). Later on she essayed writing [iliys {Julian,
1823 ; The Foscari, 1826 ; Dramatic Scenes, 1827 ; Ritnti, 182S :
Charles the First, 1828). But the prose to which she was driven by
domestic necessities lias rarer qnalitie.s than her verso. The firet
series of Our Village sketches appeared in 1824, a second in 1826,
a third in 1828, a fourth in 1830, a fifth in 1832, ami Belford Regis,
a novel in which the neighbourhood and society of Reading were
idealized, in 1835. Her Recollections of a Literary Life (1853) i»
a series oicauscrics about her favourite books. Five volumes of her
Life and Letters were published in 1870 and 1872, sliowiug her to
have been a delightful letter-miter ; two volumes of lettci-s to her
appeared in 1882.
MITHRADATES, oj, as it is often wrongly spelt,
MiTHRiDATES (i.e., " given by the god Mithras "), was a
favourite name of the Pontic kings in the third and second
centuries B.C., and was also common in Persia and the
neighbouring countries. The dynasty of Pontus was a
Persian family, claiming descent from the Achsmenid*,
and the earliest of them known in history was satrap
under the Persian empire. When that empire was destroyed
Mithradates 11. made himself king of Pontus; and ho and
his successors gradually spread their power over a great
530
M I T — M I T
part of Cappadocia and Paphlagonia. Several of them
intermarried with the Seleucidic and other Greek royal
families, and something of the Hellenic civilization was
engrafted on the native non-Hellenic character of the
kingdom. The names Mithradates, Pharnaces, and Ariobar-
zanes, all non-Hellenic, alternate in the family. The pro-
vince of Phrygia was sold in the most scandalous way by
the Roman consul Aquillius to Mithradates V., who died
probably in J 20 B.C. He was succeeded by his son
Jlithradates Eiipator, sixth of the name, one of those
remarkable conquerors that arise from time to time in the
East. He was a boy when his father died, and for seven
years lived the wandering life of a hunter pursued by
assassins. His courage, his wonderful bodily strength and
size, his skill in the use of weapons, in riding, and in the
chase, his speed of foot, his capacity for eating and drink-
ing, and at the same time his quick and penetrating
intellect, his wonderful mastery of twenty-two languages, —
all these quaUties are celebrated by the ancients to a degree
which is almost incredible. With a surface gloss of Greek
education, he united the subtlety, the superstition, and the
obstinate endurance of an Oriental. He was a virtuoso,
and collected curiosities and works of art; he assembled
Greek men of letters round him; he gave prizes to the
greatest poets and the best eaters. He spent much of his
time in practising magic arts, the interpretation of dreams,
and other superstitious ceremonies ; and it was believed
that he had so saturated his body with poisons that none
could injure him. He trusted no one; he murdered his
nearest relations, his mother, his sons, the sister whom he
had married ; to prevent his harem from falling a trophy
to his enemies he murdered all his concubines, and his
most faithful followers were never safe. He once dis-
appeared from his palace, no one knew whither, and
returned aftet'some months, havLng wandered over all Asia
Minor in disguise. "^ Except in tl" ^ pages of romance or the
tales of the Thoumiul and One Nights it would be difficult
to find anything to rival the account given of Mithradates
by the gravest of historians. These qualities/fitted him to
be the opponent of Roman arms in Asia Mi^or, to be the
cha-mpion of the East in its struggle against the destroying
and yet civilizing power of the West. He resisted the
Romans for eighteen years, yet we can hardly credit him
with much real generalship or organizing power. He
■could collect masses of men and hurl them against the
Roman legions ; everything that boundless energy and
loundIe.-is hatred could do he did ; but the strength of his
opposition to the Romans lay in the fact that all the dislike
inspired by Rome in the worst and most cruel time of her
rule was arrayed on his side.
No direct collision took place between the Romans and
Mithradates for thirty-two years, though the republic took
■away Phrygia from him in 120 B.C., and several times
th'.varted his designs in Paphlagonia and Cappadocia.
Th>3 rupture came about the time of the Social War.
Mithradates, prompted, it is said, by envoys from the Italian
allies, Uiok advantage of the intestine struggles in Italy.
War broke out in 88, on the ostensible cause of disputes
about the kingdom of Bithynia; Mithradates rapidly
overran Galatia, Phrygia, and Asia, defeated the Roman
armies, and made a general mas-sacre of the Romans
resident in Asia. He^lso sent large armies into Europer^
Greece, and his generals occupied Athen.s. But Sulla in
Greece and Fimbria in Asia defeated his armies in several
battles ; the Greek cities were disgusted by his severity,
and in 84 B.C. he concluded peace, abandoning all his con-
quests, surrendering seventy shijis, and paying a fine of
2000 talents. Iil'orena in/aded Pontus without any good
reason in 83, but was defeated in 82. Difficulties con-
^lallll^ aroso betwe^^n the two adversaries, and in 74 a
general war broke out. Mithradates defeated Cotta, one
of the Roman consuls, at Chalcedon ; but Lucullus worsted
him in several engagements, and drove him finally in 72
B.C. to take refuge in Armenia with his son-in-law Tigranes.
After two great victories in 69 and 68, Lucullus was dis-
concerted by mutiny among his troops and the defeat of
his lieutenant Fabius (see vol. xv. p. 56). In 66 he was
superseded by Pompey, v/ho completely defeated both
Jilithradates and Tigranes. The former established him-
self in 64 at Panticapsum, and was planning new
campaigns against the Romans when his own troops
revolted, and, after vainly trying to poison himself, he
ordered a Gallic mercenary to kill him. So perished the
greatest enemy that the Romans had to encounter in Asia,
Minor. His body was sent to Pompey, who buried it in
the royal sepulchre at Sinope.
MITHRAS was a Persian god whose worship spread
over the Roman world during the 2d and ,3d centuries
after Christ. His name is found in the oldest records of
the East Aryan races. In the Rig-Veda, Mitra, i.e., the
friend, and Varuna, i.e., Oi!pa!/o9, are a pair of gods regularly
associated : they denote the heaven of day and the heaven
of night. Mithras is therefore by origin the god of the
bright heaven and of day, closely related in conception to,
and yet expressly distinguished from, the sun. In the
developed Old Persian religion of Zoroaster Mithras retained
a place ; he was not one of the greatest gods, but was
first of a triad whicli, while less pure embodiments of the
divine nature, were more easy for men to comprehend and
to worship. The seventh month, which bears his name, and
the sixteenth day of every month were sacred to Mithras;
prayers were offered to him at sunrise, at mid-day, and
at sunset. When the Persians conquered Assyria and
Babylonia their religion was much affected by the worship
of these more educated races. The worship of foreign
deities was introduced, that of Persian deities was changed
in character ; and the gods were represented by images.
The cultus of Mithras now became far more prominent, ha
was identified with the sun, and an elaborate ritual with
the non- Aryan accompaniment of mysteries was established.
This revolution had begun before Herodotus (i. 131) could
identify Mithras with the Assyrian goddess Mylitta, and
it became more thorough during the 4th century B.C.
It is in this most developed form that we know the
cultus of Mithras. The god of light becomes by a ready
transition, which is made in the very oldest Aryan records,
the god of purity, of moral goodness, of knowledge. There
goes on in the world as a whole, and in the life of each
man, a continual struggle between the power of good and
the power of evil ; Mithras is always engaged in this con-
test, and his religion teaches all, men and women alike, to
aid in the battle. Victory in this battle can be gained
only by sacrifice and probation, and Mithras is conceived
as always performing the mystic sacrifice through which
the good will triumph. The human soul, which has been
separated from the divine nature and has descended to
earth, can reascend and attain unipn with God through a
process of fasting and penance which is taught in the
mysteries ; the sacrifice which is being always offered by
Mithras makes this ascent and union possible. Those
who were initiated in the mysteries of Mithras had to pass
through a long probation, with scourging, fasting, and
ordeal by water, and were then admitted as soldiers fighting
on behalf of Mithras. This was the lowest terrestrial
grade, but there were still two others to attain, the Bull
and the Lion, each involving further probation, before the
soul could rise above the earth. It then ascended by the
grades of Vulture, Ostrich, and Crow through the region
of aether ; and then it strove to become pure fire through
the grades of Gryphon, of Perse.s, and of the Sun. Finallj
M I T — M I T
531
the soul attained complete union with the divine nature
through the grades of Father Eagle, of Father Faicon, and
of Father of Fathers. A holy cave on a hill was the
central point in the worship; and the mystic rites involved
watching and fasting all night till sunrise brought the
triumph of light.
The worship of Slithras became known to the Romans
through the Cilician pirates captured by Pompey about 70
B.C. It gained a footing in Eome under Domitian, was
regularly established by Trajan about 100 A.D., and by
Comnodus about 190. Finally the mysteries were pro-
hibited and the holy cave destroyed in 378. Dedicatory
inscriptions to Dto Soli Invicto ilithrse, and votive reliefs
erf Boman work, are very common. The usual representa-
tion shows Mithras in the mystic cave performing the
mystic sacrifice; a young man in Oriental costume kneels
with one knee on a prostrate buU, grasping the head and
palling it back with the left hand, while with the right he
plunges his sword into its neck. A dog, a snake, and a
scorpion drink the blood that flows from the bull ; a crow
sits on the rock behind Mithras ; the figures of the sun
and of the moon occupy the two sides of the relief.
See Lajarde, Rwhercha sur U CulU dc UUhraa.
MITRE. See Costume, vol. vi. p. 463 ; and Heealdey,
vol. xi. p. 711.
MITSCHERLICH, En.HAnPT (1794-1863), was born
January 7, 1794, at Neuende near Jever, in the grand-
duchy of Oldenburg, where his father was pastor. He
was educated at the gymnasium of Jever under the historian
Schlossei. In 1811 he went to Heidelberg, where he
devoted himself to philology, giving special attention to
the Persian language. In 1813 he went to Paris, partly
for study, partly with the view of obtaining permission to
join a French embassy to Persia. The political events of
1814 put an end to this scheme, and Mitscherlich returned
to Germany. He then set to work on a history of the
Ghurides and Kara-Chitayens, manuscript materials for
which he found in the university library of Gottingen, and
a portion of which he published in 1815. Still anxious
to visit Persia, he resolved to study medicine in order that
he might enjoy that freedom of travel usually allowed in
the East to physicians. He began at Gottingen vrith the
study of chemistry, and this so completely arrested his
attention that he gave up the idea of the journey to Persia
and the medical profession. In 1818 he went to Berlin,
where he worked in the laboratory of Professor Link. He
made analyses of phosphates and phosphites, arseniates and
arsenites, confirming the observations of Berzelius as to
their composition. In the course of these investigations
he observed that corresponding phosphates and arseniates
crystallized in the same form.
This was the germ from which grew the theory of
isomorphism. In order to follow out his discovery
Jlitscherlich set to work to learn crystallography. His
teacher was a fellow student, Gustav Rose, to whose
penetrating mind and profound knowledge of mineralogy
have been due some of the most interesting developments
and illustrations of the theory of isomorphism. Having
measured the inclinations of the faces of a vast number of
natural and artificial crystals, he established the principles
of isomorphism very much as we now hold them.
It is right that we should remember that Mitscherlich
was not the first to notice the fact that two different sub-
stances might have the same crystalline form, or that one
element could partially replace another without great
change of form. Rom^ de I'lsle in 1772 mentions mixed
vitriols containing variable proportions of iron and copper,
and Leblanc in 1802 showed that the crystalline form
remains the same although the pjoportions vary both in
tha case of these mixed vitriols and in that of mixed
alums. Vauquelit haa already, in 1797, proved that
alum might contain variable quantities of ammonia without
any corresponding variation of crystalline form.
The authority of Haiiy, who laid down as one of his
principles that each compound has its own crystalline form,
for a time kept these observations in the background.
Further cases were, however, observed. WoUaston (1812)
accurately measured the angles of the rhombohedral
carbonates, and proved that the forms of these minerab,
although nearly the same, are not absolutely identical.
He showed that a similar close approximation to identity
exists in the case of the vitriols. Fuchs in 1815 brought
forward his theory of "vicarious constituents." Gay-'
Lussac proved that a crj'stal of common alum continues to
grow when placed in a solution of ammonia alam, and
cases of crystallized mixtures were pointed out by the
French mineralogist Beudant. But notwithstanding these
foreshadowings, of which we know, on the evidence of
Gustav Rose, that Mitscherlich was wholly ignorant, the«e
was at the time of which we are now speaking no trace of
a theory, but merely isolated observations. The theory of
isomorphism is the work of Mitscherlich. It was com-
municated to the Berlin Academy on December 9, 1819.
In that year Berzelius paid a visit to Berlin, and was so
struck with Mitscherlich's ability that he suggested him to
the minister Altenstein as the most fitting successor to
Klaproth in the chair of chemistry in that university. It
is not surprising that this idea was not carried out. It
was only four years since Itfitscherlich had begun to study
chemistry ; he had never lectured, nor had he published
anything on the subject. '
Although Altenstein did not at that time carry out the
proposal of Berzelius, he was so far impressed by it that
he obtained for Mitccherlich a Government grant to enable
him to continue his studies under Berzelius.
In 1820 he went to Stockholm, where he worked for a
year in Berzelius's laboratory. In 1822 he was appointed
extraordinary and in 1825 ordinary professor in Berlin,
In the course of an investigation into the slight differences
discovered by WoUaston in the angles of the rhombohedra
of the carbonates isomorphous with calc-spar, Mitscherlich
observed that the angle in the case of calc-spar varied with
the temperature. On extending his inquiry to other non«
isotropic crystals he observed a similar variation, and was
thus led, in 1825, to the discovery that non-isotropic
crystals, when heated, expand unequally in the direction of
dissimilar axes. In the following year he discovered the
change, produced by change of temperature, in the direction
of the optic axes of selenite. The discovery (also in 1826)
that sulphur can be obtained in two absolutely distinct
crystalline forms threw much light on the fact that the two
minerals calc-spar and aragonite have the same composition
but perfectly difierent forms. Other cases of this property,
to which Mitscherlich gave the name of dimorphism, were
arrived at not long after.
In 1833 he made a series of careful determinations of
the vapour densities of a large number of volatile substances,
and proved that Gay-Lussac's law as to the proportions
by volume in which oxygen, nitrogen, hydrogen, and
chlorine unite with one another holds generally for volatile
elements, and that the simplicity of the relation of the
volume of the compound to that of the component gases is
also general.
In pure chemistry Mitscherlich's discoveries were mainly
connected with isomorphism. Thus he obtained selenic
acid in 1827, and showed the isomorphism of its salts with
the sulphates, and examined with great care the manganates
and permanganates, showing their isomorphism with the
sulphiates and with the perchlorates respectively. But he
did much important work unconnected with this special
M I T — ii N E
iiubject. We may in particular refer to his discovtry of
the relation of benzene to benzoic acid, of nitro-benzene,
and of a considerable munber of the derivatives of benzene.
In 1833 he published his Lchrbuch dcr Chunie,, a
student's text-book of chomistrj' of the most thoroughly
practical and yet rigidly scientific kind, from the study of
which teachers of chemistiy may still derive many a
Taiuable hint. His interest in mineralogy led him to the
jr.tudy of the geo'ogy of volcanic regions, and he made
frequent -^Tsits to the Eifel ■\vith a view to the discovery of
t, theory of volcanic action. He did not, however, publish
any papers on the subject, but suice his death his notes
have been arranged and published by Dr Roth in the
^Memoirs of the Berlin Academy (1S66). In December
-SGI symptoms of heart disease made their appearance,
1 ut he was able to carry on his academical work till
}Jecember 1862. He died at Schoneberg near Berlin on
; bth August 1863.
ilitscheriich's publislied paperB are chiefly to be found in tlie
Abliandlu'iiQCH' of the Berlin Academ}', in PoggendoTjTs Annalcn,
tnd in the Anrialcs dc Chimic et dc Plnjsiquc, The fourth edition
c f the Lehrbuch der Chetnic was published in 1844 ; a fifth was
1 egun in 1S55, but was not completed. (A. C. B.)
MITYLENE, or Mytilene. See Lesbos.
MIZPAH (nBVD) and IhzpzS ("Eyp) are Hebrew words
for a "place of prospect," or high commanding poini.
The cities of Palestine generality occupied such positions ;
and so in the Old Testament we find several places bearing
the name of " The Mizpah '' (Mizpeh). Sometimes a
determining genitive is added ; " The Mizpeh of Gilead "
(Judg. xi. 29), "The Mizpeh of Moab" (1 Sam. xxii. 3).
(1) The most famous of these places is that in Gilead, a noted
eanctuary (Judg, xL 11 ; Hosea v. 1), claiming consecration from
the sacrifice of Jacob (Genu xxxi. 54) and the vias^ebci or sacred
etone erected by him (ver. 46). The narrative of Gen. xxxi. 45 sq.
is -Eomewbat obscure, and not all from one hand. We gather,
however, from it that another name of '*The Mizpah" was Galeed,
i.e., Gilead. Thus Mizpah, Mizpeh Gilead, GUead (Hos, vi, 8),
Ramath Mizpeh {i.e., the height of Slizpeh, Josh, xiiL 26), and
Ramoth Gilead (the heights of Gilead), or simply The Raraah (2
Kino;9 viii, 28, 29), are almost universally taken to be one place,
,With this it agrees that Ramoth Gilead was a city of refuge, which
points to an early sanotit)'. The place is prominent thi-oughont the
hJBtory, It was the seat of Jephthah (Judg, xi,), the mourning for
whose daughter probably gives us a glimpse into the ancient rites
of a provincial sanctuary, the residence of one of Solomon's officers
(1 Kaogs iv, 13), and a hotly disputed frontier city in the wars
between Syria and the house of Omri, before which Allah fell (1
Eijigs .X.-S ii, ), and in which the military revolt of Jehu was organized
(2 Kings ix.), Maspha was still a strong place in the Greek period,
and was taken by Judas Maccabeeus (1 Mac. v, ZU), Euscbius knows
Ramoth as a place 15 miles west of Philadelphia or Kabbah of
Animon, It is therefore commonly identified ivith El-Salt, the
modem capital of the Belkil; but this cannot be said to be made
out, (2) The BoDJamite Mizpah or Mizpeh, also a sanctuary, is
often named in the history of Samuel. It was a border fortress of
King Asa (1 Kii;;^3 xv, 22), and the residence of Gedaliah as governor
of Judffla after the fall of Jerusalem (Jer, xl,). Its old sanctity was
still remembered in the Maccabee times, and from 1 Mac, iii, id we
conclude that it commanded a view of Jerusalem. The most prob-
able identification is with the prominent hill-top of Neby Samwil,
There was (3) another Mizpeh in the low country of Judah (Jo.'^h,
XV, 38), and (4) a laud or ^aUey of Mizpeh (Josh, xi 3, 8) under
Jlount Hermon,
MNEMONICS, or artificial helps to the memory, have
been employed in a more or less systematic form from a
(very early period. Mnemonics (ro fivrjiioviKov, sc. Tixv-qf-a-
or TupayyiXjxa) were much cultivated by Greek sophists
and philosophers, and are repeatedly referred to by Plato
and Aristotle, In later times the invention was ascribed
to the poet Simonides,' perhaps for no other reason than
that the strength of his memory was famous, Cicero, whp
attaches considerable importance to the art, but more to
the principle of order as the best help to memory, speaks
' PlSny, n. JV,, rii, 24, Cicero, De Or., il. 86, mentions lliis tslicf
vithout committing himself to it
of Carncados (or perhaps Charmadei) of Athens and Metro-
dorus of Scepsis as djstiriguished examples of the use of
wsU-ordered images to aid the memory. The latter is
f;aid by Pliny to have carried the art so far ut nihil noji
iisdem verbis redderet auditum. The Romans valued such
helps as giving facility in public speaking. The method
u.sed is described by the author of Ehet. ad ITeren., iii. li>
24; see also Quintilian (iTist. Or., x. 1, 2), whose account is,'
however, somewhat incomplete and obscure. In bis time
the art had almost ceased to be practised, "The Greek and
Roman system of mnemonics was founded on the use cf
mental places and signs or pictures. The thing to be re-
membered was localized in the imagination, and associated
with a symbol which concretely represented what it was
desired to retain in the memory, special care being taken
that the symbols should be as vivid, pleasing, and impres-
sive as possible. The most usual method was to choose
a large house, of which the apartments, walls, windoivs,
statues, furniture, &c., were severally associated with cer-
tain names, phrases, events, or ideas, by means of symbolic
pictures ; and to recall these it was only necessary to seajch
over the apartments of the house, till the particular place
was discovered where they had been deposited by the ima^
gination. As the things td be remembered increased, new
houses could ba built, each Eet apart to a certain class of
ideas or events, and these houses were again constructed
into a mnemonic town. In accordance with this system,
if it were desired to fix an historic date in the memory, it
was localized in an imaginary to'mi divided into a certain
number of districts, each with ten houses, each house with
ten rooms, and each room with a hundred quadrates or
memory-places, partly on the floor, partly on the four wall-Sj
partly on the roof. Thus, if it were desired to fix in thd
memory the date of the invention of printing (1436), an
imaginary book, or some other symbol of printing, would
be placed in the thirty-sLxth quadrate or memory-place
of the fourth room of the first house of the historic district
of the town. The success of the method depended largely
on the power of the imagination to give the diS"erent houses,
rooms, &c., characteristic varieties of aspect, and we may
suppose that it was the effort to frame suitable images and
places, giving an adventitious interest to dry details, that
constituted the real advantage of the system. Except that
the rules of mnemonics are referred to by Martianus
Capella, nothing fm-ther is known regarding the practice
of the art until the 13th centmy, when the system of the
Romans was revived and a good many treatises ' were
published on the subject. Among the voluminous writ-
ings of Roger Bacon is a tractate De Arte Memorativa,
which exists in JIS, at Oxford, Raymond Lully devoted
special attention to mnemonics in conneidon with his an
fjfcneralis. . The first important modification of the method
of the Romans was that invented by Conrad Ccltes, al
German poet, who, in his Epitoma in utramque Ciceronis
rhetoricam cum arte memorativa nova (1492), instead of
places made use of the letters of the alphabet. About
the end of the 1 5th century Petrus de Ravenna awakened
such astonishment in Italy by his mnemonic feats that he
was believed by many to be a necromancer. His Phoenix
Artis MeKwriw, pubUshed at Venice in 1 491 in four volumesj
went through as many as nine editions, the seventh appear-
ing at Cologne in 1608, An impression equally great was
produced about the end of tho 16th century by Lambert
Schenkel, who taught mnemonics in France, Italy, and
Germany, and, although he was denounced as a sorcerer by
the university of Louvain, pubb'shed in 1593 his tractate
De Mcmoria at Douai %vith the sanction of that celebrated
theological faculty, Tho most complete account of his sy,s-
tcm Ls given in two works by his pupil Martin Sommcr, pub-
lished at Venice in 1G19. Giordano Bruno, in connexion
M O A — M O A
533
■with his exposition of the ars tfeneroKs of Lully, inoiudcd
a memona (cchnica in his treatise De Umbrii Idearum.
About the middle of the 17th century Winckelmann made
known what he called the " most fertile secret " in mne-
monics, namely the use of Isttars with figures so as to express
numbers by words ; and the philosopher Leibnitz adopted
an alphabet very similar to that of Winckelmann in con-
nexion with his scheme for a form of "JTritiag common to all
languages. Winckelmann's method vras modified and sup-
plemented in regard to many details by Richard Grey, who
published a Memoria Technica in 1730. The principal
part of Grey's method is briefly this : " To remember any-
thing in history, chronology, geography, <fec., a word is
formed, the beginning whereof being the first syllable or
syllables of the thing sought, does, by frequent repetition,
of course draw after it the latter part, which is so contrived
as to give the- answer. Thus, in history, the Deluge
happened in the year before Christ two thousand three
hundred forty-eight ; this is signified by the word Delrfoi,
Del standing for Deluge and etoh for 2348." To assist in
retaining the mnemonical words in the memory they were
formed into memorial lines. The vowel or consonant
which Grey connected with a particular figure wzs chosen
arbitrarily ; but in 1806 Feinaigle, a monk from Salem
near Constance, began in Paris to expound a system
of mnemonics, one feature of ■which was to represent the
numerical figures by letters, chosen on account of some
similarity to the figure to be represented or some accidental
connexion with it. This alphabet was supplemented by
a complicated system of localities and signs, with the aim
of expressing, by a more vivid and impressive symbol, ideas
which for want of this are apt to pass from the memory,
and of establishing between ideas of the same group an
intimate relation, so that the mention of the one would sug-
gest the other. Feinaigle, who published a Notice sur la
mnimonique at Paris in 1805, came to England in 1811,
and in the fallowing year published The New Art of
Memory. A simplified form of Feinaigle's method was
published in 1823 by Aim6 Paris,' and the use of symbolic
pictures ■was revived in connexion with the latter by a
Pole, Jazwinsky, of whose system an account was pub-
lished by J. Bem, under the title Expose General de la
Metkode Mnemonique Polonaise, perfectionnee A Paris, Paris,
1839. Various other modifications of the systems of
Feinaigle and AimA Paris were advocated by subsequent
mnemonists, among them being the Phrenotyping or
Brain-Printing method of Beniowsky, the Phreno-Mnemo-
techny of Gouraud, and the Mnemotechuik of Carl Otto,
a Dane. The more complicated mnemonic systems have
fallen almost into complete disuse ; but methods founded
chiefly on the laws of association have been taught with
some success in Germany by, among others, Kothe, who is
the author of Lehrhtich da- Mnemonik, and Katechismus
der Geditchtnisskmist, both of which have gone through
several editions ; and in England by Dr. Ed^ward Pick,
whose Memory and the Rational Means of Improving it
has also obtained a wide circulation. In certain cases
mnemonical devices may be found of considerable service ;
but all systems which have aimed at completeness have
been found rather to puzzle than aid the memory. The
fullest history of mnemonics, is that given by J. C. F. von
Aretin in his SystematUche Aideitung zvr Theorie U7id
Praxis der Mnemonik, 1810.
MOA. See Dinornis.
MOAB. Moab and Ammon (children of Lot) consti-
cute along with Edom and Israel (children of Isaac) that
group of four Hebrew peoples which in early antiquity had
issued from the Syro-Arabian ■wilderness, and settled on
the border of the cultivated country eastward of the great
depression which extends from the Gulf of Elath to tha
Dead Sea, and up the valloy of the Ji-)rdin. .\cr?:-J'Dg to
the book of Genesis, they had 3omo out of Mesopotamia,
and- 30 were precursors of ths larger -wave wliich followed
from the same quarter, forming the most southern outpost
of the AramaM.n immigration into the lands of Canaan
and Heth. Whether the Hebrews were originally .Ara-
maeans is questionable, but it is certain that, like the
Aramaeans, they were distinct from the Canaanites, whose
conquerors they were. Such was the relation of the old
and new inhabitants, not only in Western Palestine after
the Israelite occupation, but also, and from a muoh earlier
period, in Eastern Palestine, where the aborigines were
-Amorites — that is, Canaanites — and vrhere the Bne Ammon
and Moab and the Bne Isaac successively settled in their
lands. The old population did not disappear before the
conquerors, but continued to subsist among them. In
a considerable district — namely, in Gilead — the Amorite-s
even remained unsubdued, and thus formed a gap, only
imperfectly filled up by the Bne Ammon, between the
Hebrew line of immigration on the south and the Ara-
maean line more to the north, — a gap which did not begin
to close until the historical period. From this district
they even endeavoured, and with some success, as ■wiU be
afterwards seen, to recover the territory which had been
taken from them in the south. But where they were the
subjects of the Hebrews they constituted the basis of the
population, the mainstock of the working and trading
classes. The extent of their influence over the conquerors
may be judged from the fact that it was their speech
which gained the upper hand. The Moabites, and doubt-
less also the Ammonites and Edomites, spoke the language
of Canaan as well as the Israelites. They must have
learned it from the Canaanites in the land eastward of
Jordan, prior to the period at which Jacob immigrated to
and returned from Egypt. Our knowledge is extremely
imperfect as regards other departments of the Canaanite
influence ; but in religion it has left a noticeable trace in
the cultus of Baal-Peor, which was carried on in Moabita
territory, but was certainly of Canaanite origin.
The assumption that the change of language was first hrougtt
about by the Israelite^ in the land which is called by preference
that of Cauaan, is rendered untenable by the fact that the Moabittts
also spoke Canaanitish. It is vain to urge against the identity of
Hebrew and Canaanitish th^ distinction between Phcenician and
Hebrew ; for doubtless similar distinctions existed between the
dialect of the Phoenician coast towns and that of the Hivites,
-Amorites, and Cauaanitcs generally, whose language the Hebrews
borrowed. That the Aramaeans of Damascus, who also were com-
pelled to mingle \vith the Hethites in the country of which they
had taken possession, nevertheless retained their original tongue is
to be explained by the circumstance that they continued to maintaic
direct relations with the mother-eountry of Mesopotamia, and mora-
over had greater internal cohesion. The designation Amorites,
usually given in the Old Testament to the original inhabitants
of Eastern Palestine, is substantially synonymous with that of
Canaanites, although not quite so comprehensive. The Palestine
of the Pre-Israelitio period, which in the Pentateuch is called the
Land of Canaan, figures in -Amos as the Land of the Amorites.
While, however, the former name is bestowed chiefly upon that
portion of the earlier population which had remained unconquered,
the latter is given to the portion against which the Israelites first
directed their attack and in wboeo territory they settled. This took
place in the mountain district, first to the east .%nd afterwards to the
west of Jordan. For this reason the Amorites, as contrasted with
the Canaanites of the cities of the level country, are a highland
race, like the Hebrews themselves, but belong exclusively to the
past. In the time of the Biblical narrators, the Canaanites are stOl
living here and there in the land, but the Amorites have once lived
where the Israelites now are. This explains the fact that, while in
ordinary peaceful circumstances the Canaanites are named as the
old inhabitants, the .Amorites are immediately substituted for them
wherever war and conquest are spoken of. Sihon and Og, with
whom Moses does battle, are kings of the Amorites ; in like manner
it is with the twelve kings of the Amorites that Joshua has to deal
westward of the Jordan. The Amorites as an extinct race of cotirso
-•xssume a half-mythical character, and are represented as giants, tuU
as cedars and strong as oaks.
■)34
M O A B
Just as Israel was the people of Jehovah, and Ammon
the people of Milcom, Moab was the people of Chemosh
(V)03, Num. ijd. 29). The kingship of Chemosh was
regarded as thoroughly national and political in its char-
acter, but did not on that account exclude the institution
of a human king, which existed in Moab much earlier than
in Israel ; in the time of Moses the Moabites had a king,
and the institution was even then an old one. The capitals
of the kingdom were Ar-Moab and Kir-Moab, south from
the Amon ; these were not, however, the constant residences
of the kings, who continued to live in their native places,
sls, for example, Mesha in Dibon. Doubtless there were
changes of dynasty, and traces exist of a powerful aristocracy
(Ariele Moab ; 2 Sam. xxiii. 20).
The land of the Moabites, the Balkd, is bounded north-
ward and southward by Mount Gilead and Wadi 'l-AhsA,
westward and eastward by the Dead Sea and the Wilder-
ness ; it is divided into two portions by the deep bed of
the Amon, that to the north being the more level (Mishor),
and that to the south being more broken up, and consti-
tuting the proper stronghold of the nation. The soil is
peculiarly adapted for sheep-farming (2 Kings iii) and the
culture of the vine (Isa. xvi.).^
The historical importance of the Moabites lies wholly in
their contact with Israel, and we have no knowledge of
them apart from this. After the Israelites had quitted
Egypt and passed a nomadic life for about a generation in
the neighbourhood of Kadesh, they migrated thence, still
under the leadership of Moses, into northern Moab, dis-
possessing the Amorites, who had made themselves masters
of that district. The interval from Kadesh to the Amon
could be passed only by a good understanding with Edom,
Moab, and Ammon, — a proof that the ethnical relationships,
which at a later period were expressed only in legend, were
at that time stiU living and practical. In all probability
the Moabites called the Israelites to their aid ; they were
not as yet aware that this little pastoral people was des-
tined one day to become to them a greater danger than
the Canaanites by whom , they were threatened at the
moment.^
As the story of Balaam indicates, the Moabites would
willingly have been rid of their cousins after their service
had been rendered, but were unable to prevent them from
settling in the land of Sihon. The migration of the tribes
of Israel into Western Palestine, however, and the dissolu-
tion of their warlike confederation soon afterwards made a
restoration of the old frontiers possible. If King Eglon
took tribute of Benjamin at Jericho, the territory between
Amon and Jordan must also have been subject to him, and
^ Tliere does not seem to have been any difference in this respect
between tlie northern and Eoiitheni portions ; jnstead of Heshbon,
Sibmah, and Jaezer(Isa. xvi.), the poet Hatim of Tayyi, a tittle before
Mohammed, names Maab and Zoar as the chief wine centres (Yakut,
i». 377, 19).
' The facts as a whole are indubitable ; it cannot be an invention
that the Israelites settled first ia Kadesh, then in northern Moab, and
thence passed into Palestine proper. The only doubtful point is
whether the song in Num. xx\. 27 sqij. is contemporary evidence
of these events.- It is cert-ainly not a forgery, but it is a ques-
tion whether it really refers to the destruction of the kingdom of the
Amorites at Ueshbon. This reference rests entirely upon the words
IID'D *"IDN TIPdS, which niijht very well bo omitted as a mere gloss,
ill which cnse the song would naturally bo understood as directed against
the Moabites themselves ; it is in this last sense that it is taken by the
author of Jcr. xlviii. (Comp. E. Meyer In Stade's Zcitschr. f. A Tliclie
Wisscnsch., 1881, p. 129 S57.) As Israel got the better of the Amorites
on the plain of Moab, so did Hadad king of tho Edomites vanquish the
Midianites on tho "field" of Moab (Gen. xixvL 35) ; this took place
in Gideon's time, as is bor.ic out by tho fact that between Hadad and
the downfall of iho mcwvX Edoniile monarchy, i.e. to the period of
David, there weio four reigning princes. Conlusod recollections of a
fnriiier settlement of the Midianites in northern Uoab are seen in
Nnm. xxii. •), 7; -::v. IS
Reuben must even then have lost his land, or at least his
liberty. It would appear that the Moabites next extended
their attacks to Mount Gilead, giving their support to the
Ammonites, who, during the period of the judges, were its
leading assailant.s. So close was the connexion between
Moab and Ammon that the boundary between them vanishes
for the narrators (Judges xi.).
Gilead was delivered from the Ammonites by Saul, who
at the same tim« waged a successful war against Moab ; the
fact is lightly touched upon in 1 Sam. xiv. 47, as if this
were a matter of course. The establishment of the mon-
archy necessarily involved Israel in feuds with its neighbours
and kin. The Moabites being the enemies of the Israelite
kingdom, David naturally sent his people for shelter thither
when he had broken wdth Saul ; the incident is precisely
analogous to what happened when he himself at a later
period took refuge from Saul's persecution in Philistine
territory, and needs no explanation from the book of Buth.
As soon as he ceased to be the king's enemy by himself
becoming king, his relations with Moab became precisely
those of his predecessor. The war in which apparently
casual circumstances involved him with Hanim ben Nahash
of Ammon really arose out of larger causes, and thus spread
to Moab and Edom as weU. The end of it was that all
the three Hebrew nationalities were incorporated with the
kingdom of Israel ; the youngest brother eclipsed and sub-
dued his seniors, as Balaam had foreseen. Through the
work of Saul and David the political system of Palestine
was altogether changed : the smaller peoples were no longer
a match for Israel, which established a decisive prejKinder-
ance, and transformed what had hitherto been jealousy on
the part of Moab and Ammon as well as of Edom into
bitter hatred ; this hatred did not cease even after nothing
but a religious shadow remained of what had once been the
political supremacy of the people of Jehovah.
The struggle with Ammon which David began ultimately
assumed larger dimensions, and brought the Aramaeans
also into the field against him. He was successful, indeed,
against them also, and destroyed their most powerful
kingdom ; but after his death they recovered themselves,
and pressed steadily on from the borders of the wilderness
towards the sea ; at their head were those kings of Damascus
who had established themselves on the ruins of Zoba. In
presence of these enemies the already fading distinction
between the ruling and the subject nationality within the
kingdom of Israel now completely disappeared ; and even
towaids the Canaanites outside the relations of the kings
became friendly. It is in one instance expressly stated
that the common danger threatening from the East had
to do with this (2 Sam. viii. 9 sqq.). But, conversely, it
was natural that Ammon and Moab should make common
cause with the Arama-ans ; such an attitude was suggested
by geographical jiosition and old connexions, but above
ail by their helpless fury against Israel. Both nationalities
must have succeeded in emancipating themselves very soon
after David's death, and only now and then was some strong
king of Israel able again to impose the yoke for a time, not
upon the Ammonites indeed, but upon Moab. The first to do
so was Omri, who garrisoned a number of their towns and
compelled the king to acknowledge Israel's suzerainty by
a yearly tribute of sheep, — a state of matters which con-
tinued until the death of Ahab ben Omri. But when that
brave king fell in battle with the Aramaeans at Kamoth
Gilead (about 850 B.C.), Mesha of Dibon, then tho ruler
of Moab, seized the favourable opportunity to make him-
self and his people independent. In his famous inscription
he tells how, throu;.'h tlie v.rath of Chemosh, the land had
fallen into the enemy's power and endured forty years of
slavery, and how by the grace of Chemosh the yoke is now
broken and the Israelites ignominiously driven off. In.
M O A B
535
the Bible we find only the curt statement that Moab
rebelled against Israel after the death of Ahab (2 Kings i.);
on the other hand, there is a fvdl narrative of a later attempt
on the part of Joram ben Ahab to bring Mesha again
into subjection — an attempt which promised very well at
first, but ultimately failed completely. Joram's invasion
took place not from the north- but (probably very unex-
pectedly to the enemy) from the frontier of Edom over
the Wadi '1-Ahs4; he marched through Judah and Edom,
and the kings of those countries served as auxiliaries.
He defeated a Moabite army on the frontier, penetrated
into the country and laid it wast« ; he laid siege to the
fortress of Kir-Moab so closely as to reduce it to great
straits, tut these straits seem to have filled the besieged
^vith a desperate courage, for the fortunes of war suddenly
changed. The Israelites were compelled to retir« home-
ward, a great wrath (of Jehovah) having come upon them,
that is, a severe disaster having befallen them, which is
not described, but, from the nature of the case, must have
been a sudden surprise and defeat by the enemy.'
As the Moabites owed their liberation from Israelite
supremacy to the battle of Bamah — that is, to the
Aramseans — we accordingly find them (as well as the
Ammonites) afterwards always seconding the Aramaaans in
continual border warfare against Gilead, in which they
took cruel revenge on the Israelites. With what bitterness
the latter in consequence were wont to speak of their
hostile kinsfolk can be gathered from Gen. xix. 30 sqq. —
the one trace -of open malice in the story of the patriarchs,
and all the more striking as it occurs in a narrative of
which Lot is the hero and saint, which therefore in its
present form is of Moabite origin, although perhaps it has
a, still older Canaanite nucleus. Of these border wars
we learn but little, although from casual notices it can be
seen (2 Kings yiii. 20 ; Amos L 13 ; comp. 2 Kings v.
2) that they were long kept up, although not quite
uninterruptedly. But when at length the danger from
the Aramaeans was removed for Israel by tie inter-
vention of the Assyrians, the hour of Moab's subjection
also came ; Jeroboam IL extended his frontier over the
eastern territory, as far as to the brook of the willows
^Wadi '1-Ahs4). (Perhaps the song of Num. xxL 27 sqq.
Jias reference to these events.) A vivid picture of the
confusion and anguish then prevalent in Moab has been
preserved to us in the ancient prophecy of Isa. rv., xvi.,
ivhich indeed would have greater historical value if we
were able to tell precisely what in it depicts the present.
And what is prediction of the future.^
This utterance of an older prophet was repeated some
* The narrative of Mesha in his inscription h.TS, etrange to say, not
onfrequently been regarded as parallel with 2 Kings iii., andthe con-
dasiOQ been drawn that the Biblical narrative completely inverts the
true state of the case, — it is diiBciilt to see for what motives, for there
M no braggadocio in 2 Kings iii. But it is perfectly clear that the
Jlarrative of 2 Kings iii. presupposes the revolt of Mesha as an old
affair ; while, en the other h.and, Mesha's story on the stele in the
lonvre is a narrative of this very revolt and its immediate consequences ;
jl is accordingly to be regarded as paitillel with 2 Kings L 1. Elisha's
miracle in Wadi 'l-Ahsa (2 Kings iii 16) is explained by the locality ;
Ahsa means a sandy ground with moist subsoil, where, by digging
♦reaches, water is always obtainable. The (probably compulsory) par-
ticipation of the king of Edom in Joram's expedition against Moab
jnay perhaps be brought into connexion with the fact that- the Moabites
burned to lime the bones of a king of Edom (Amos ii. 1).
* In Isa."xv. xvi. it is presupposed that the attack upon Moab has
V-en made from the north, at a time when Judah is a comparatively
* jjowerful kingdom, exerci-sing sovereignty over Edom also, and in a
P'.sition to afford shelter to the fugitive Moabites, thus not being
itself at war with them. These marks taken together can only apply
to the period of Jeroboam II. and Uzzialu Hitzig will have it that
Jonah ben Amittai wrote Isa. xv. xvi. ; but accoixiing to 2 Kings xiv.
U5 that proi'hct preached prosperity to Jeroboam, and not di^^aster
4P *^ MnabitAs.
decennia later by the prophet Isaiah, with the addition of
a clause adapting it to his time, to the effect that the
Assyrians would carry out in all it.s fulness the hitherto
imperfectly-executed threat. The Assyrians actually sub-
•jugated the Moabites, as well as the other small peoples of
that region ; but the blow was apparently not so grave as
Isaiah had predicted. They lay more out of the way than
their western neighbours, and perhaps their resistance to
the scoiu'ge of God was not so obstinate as to demand the
sharpest measures. What made it all the easier for them
to reconcile themselves to the new situation was the fact
that the Israelites stiifered much more severely than they.
From these their deadly enemies thej' were henceforth for
ever free. They did not on that account, however, give up
their old hatred, but merely transferred it from Israel to
Judah. The political annihilation of the nation only inten-
sified in Jerusalem the belief in its religious prerogative, and
against this belief the hostility of neighbours was aroused
more keenly than ever. The deepest offence at the reli-
gious exclusiveness of the people of Judsea, which then
first began to manifest itself, was, as is easily understood,
taken by their nearest relatives, Edom and Moab. They
gave terrible expression to their feelings when the Chal-
daeans urged them on like uncaged beasts of prey against
the rebellious Jews ; and they joined loudly in the general
chorus of malignant joy which was raised over the burning
of the temple and the ruin of the holy city.'
" Because Moab saith : Behold the house of Judah is
like all the other nations, therefore do I open his land to
the Bne Kedem," says the. prophet Ezekiel (xxv. 8 sqq.).
His threat against the Moabites as well as against the
Edomites and Ammonites is that they shall fall before the
approach of the desert tribes. Probably in his day the
tide of Arabian invasion was already slowly rising, and
of course it had first to overtake the lands situated on the
desert border. At all events the Arab immigration into
this qtiaxter began at an earlier date than is usually
supposed ; it continued for centuries, and was so gradual
that the previously - introduced Aramseizing process
could quietly go on alongside of it. The Edomites gave
way before the pressure of the land-hungry nomads, and
settled in the desolate country of Judah ; the children of
ix)t, on the other hand, appear to have amalgamated with
them, — ^the Ammonites maintaining their individuality
longer than the Moabites, who soon entirely disappeared.
Israel and Moab had a common origin, and their early
history was similar. The people of Jehovah on the one
hand, the people of Chemosh on the other, had the same
idea of the Godhead as head of the nation, and a like
patriotism derived from religious belief, — a patriotism
capable of extraordinary eflforts, and which has had no
parallel in the West cither in ancient or in modern times.
The mechanism of the theocracy also had much that was
common to both nations ; in both the king figui-es as the
deity's repi'esentative, priests and prophets as the organs
through whom he makes his commvmications. But, with
all this similarity, how different were the ultimate fates
of the two ! The history of the one loses itself obscurely
and fruitlessly in the sarid ; that of the other issues in
eternity. One reason for the difference (which, strangely
enough, seems to have been felt not by the Israelites alone
but by the Moabites also) is obvious. Israel received no
gentle treatment at the hands of the world ; it had to carry
on a continual conflict with foreign influences and hostile
' Zeph. it 8 sq. ; 2 Kings xxiv. 2, and Jer. xii. 9 sgq. ; Ezek. xxv.
8 aqq. It need hardly be said that the Mo-lbites shared the fate of all
the Palestinian peoples when supremacy passed from the Assyrians
to the Chaldeans, and that, notwithstanding their hatred of the Jews,
they had no difficulty in seeking allianccs'with them, when occasion*
arose on which they could be made useful (Jcr. ixvii. 3).
536
M O A L L A K A T
powers ; and this perpetual struggle with gods and men
was not profit!es3, although the e:£temal catastrophe was
inevitable. Moab meantime remained settled on his lees,
and was not emptied from vessel to vessel (Jer. xlviii. 11),
and corruption and decay were tha result. This explana-
tion, however, does not carry us far, for other peoples with
fortunes as rude as those of Israel have yet tailed to
attain historical importance, but have simply disappeared.
The service the prophets rendered at a critical time, by
raising the faith of Israel from the teuijioral to the eternal
sphere, has already been spoken of in the article Issakl.
Sources.— Tho Old Testament (RutU and Chronicles, however,
Ixing of no historical worth in this coimc.tion), and the inscription
of Mcsha, on tlio stone of Dlbon, discovered in 1868, and now in
tlio Louvre. The Berlin MoaUtica are valueless, — Schlottmann
himself, the unshaken champion of their genuineness, conceding
that they are mere scribbling, and do not even form words, much
lias sentences. The literatnre of the subject is to be found in the
commentaries on the Old Testament books, and in those on tho
inscription of Meslia. (J. WE.)
MO'ALLAKAT. Al-Mo'allaMt is the title of a group
of seven longish Arabic poems, which have come down to
us from the time before Islam. The name signifies " the
suspended" (pi.), the traditional explanation being that
these poems were hung up by the Arabs on or in the
Ka'ba at Mecca. The oldest passage known to the writer
where this is stated occurs in the 'IM of the Spanish Arab,
Ibn "Abd-Rabbih (a.d. 861-940), BilUk; ed. vol. iiL p. 116
sq. We read there : " The Arabs had such an interest in
jKietry, and valued it so highly, that they took seven long
pieces selected from the ancient poetry, wrote them in gold
on rolls (!) of Coptic cloth, and hung them up ('alia/cat)
on the curtains which covered the Ka'ba. Hence we speak
of ' the golden poem of Amraalkais,' ' the golden poem of
Zohair.' The number of the golden poems is seven ; they
are also called ' the suspended' (al-Mo'allakdt)." Similar
statements are frequent in later Arabic works. But agaiust
this we have the testimony of a contemporaiy of Ibn ".\bd-
Rabbih, the grammarian NahhAs (oft. a.d.' 949), who sajra
in his commentary on the Mo'alla^At : "As for the a8sertic>n
thnt. they were hung up in [«ii] the Ka'ba, it is not known
to any of those who have handed down ancient poems." '
This cautious scholar is unquestionably right in rejecting
a story so utterly unauthenticated. The customs pf the
Arabs before Mohammed are pretty accurately known to
us ; we have also a mass of information about the affairs
of Mecca at the time when the Prophet arose ; but no trace
of ..this or anything like it is found in really good and
ancient authorities. We hear, indeed, of a Meccan hanging
up a spoil of battle on the Ka'ba (Ibn HishAm, ed. Wiis-
tenfeld, p. 431). Less credible is the story of an important
document being deposited in that sanctuary, for this looks
like an instance of later usages being transferred to pre-
Liiamic times. But at all events this is quite a different
thing from the hanging up of poetical manuscripts. To
account for tho disajipearance of the Mo'allakAt from the
Ka'ba wo are told, in a passage of late origin (De Sacy,
Chrestom., ii. 480), that tiey were taken down at the cap-
ture of Mecca by the Prophet. But in that ca.se we should
expect some hint of the occurrence in the circumstantial
biographies of the Prophet, and iu tho works on the history
o£ Mecca ; and we find no such thing. That long poems
were written at all at that remote period is improbable in'
the extreme. All that wo know of the diffusion of Arabic
poetry, even up to a time when the art of writing had
become far mora general than it was before the spread of
Islam, points exclusively to oral tradition. Moreover, it
is quite inconceivable that there shoilld have been either a
guild or a private individual of such acknowledged taste.
' Br'st Frunkel, An-KatOuis' Commailit/- si<r Mu'allaiia rf."s Iw-iil-
Quis (HaLc 'S'B). n. viii."
or of SUCH influence, as to bring about a consensus of
opinion in favour of certain poems. Think cf the mortal
offence which the canonization of one poet mast hare given
to his rivals and their tribes ! It was quite another thing
for an individual to give his own private estimate of the
respective merits of two poets who had appealed to him o.s
umpire ; or for a number of poets to appear at large gather-
ings, such as the fair of 'Okiz, as candidates for the placid
of honour in the estimation of the throng which listened
to their recitations. In short, this legend, so often retailed
by later Arabs, and still more frequently by Europeans,
must be entirely rejected.* The story is a pure fabrication
based on the name " suspended." The word was taken in
its literal sense ; and as these poems were undoubtedly
prized above all others in after times, the same opinion
was attributed to " the [ancient] Arabs," who were sup-
posed to have given effect to tneir verdict in the way
already described. A somewhat simpler version, also
given by NaldiAs in the passage akeady cited, is as follows :
" Most of flie-Arabs-werij accustomed to meet at 'OkAz and
recite verses ; then if the king was pleased with any poem,
he said, 'Hang it up, and preserve it amongluj liea-rares.' "
But, not to mention ofher difficulties, there was no king of
all the .(Vrabs ; and it is hardly probable that any Arabian
king attended the fair at 'Okiz. The story that ohe poems
were written in gold has evidently originated in the name
"the golden poems" (literally "the gilded"), a figurative ex-
pression for excellence. We must interpret the designation
" suspended " on the same principle. In all probability it
means those (poems) which have been raised, on account of
tJieir value, to a specially honourable position. Another
derivative of the same root is 'ilk, " precious thing."
The selection of these seven poems can scarcely have
been the work of the ancient Arabs at all. It is much
more likely that we owe it to some connoisseur of a later
date. Now Nalihis says expressly in the same passage :
" The true view of the matter is this : when HammAd
arrAwiya (Hammid the Rhapsodist) saw how little men
cared for poetry, he collected these seven pieces, urged
f.eople to -study them, and said to them : ' These are the
poems] of renown.' " And this agrees with all oiu' other
information. HammAd (who lived in the first three quar-
ters of the 8th century a.d.) was perhaps of all men the
one who knew most AJabic poetry by heart. The recita-
tion of poems was his profession. To such a rhapsodist
the task of selection is in every way appropriate ; and it
may be assumed that he is responsible also for the some-
what fantastic title of "the suspended."
The collection of HammAd appears to have consisted of
the same seven poems which are found in our modern
editions, composed respectively by AmraaUfai.s, Tarafa,
Zohair, Labid, 'Antara, 'Amr ibn Kolthilm, and HArith
ibn Hilliza. These are enumerated both by Ibn "Abd-
Rabbih, and, on the authority of the older philologists, by
NahhAs ; and all subsequent commentators seem to follow
them. We have, however, eWdence of the existence, at
a very early period, of a slightly different arrangement.
Two of the foremost authorities in Arabic poetry are Abii
'Obaida and Mofaddal, — men who for care and accuracy
in preserving the genuine text were far ahead of their much
older contemporary HammAd. Both of these inserted a
poem by NAbigha and one by A'shA in place of those of
'Antara and HArith ; ' and, if our infonnant has expressed
' Doubts had alrcnily been exprcsatd by various scholars, -vybfu
Heiigstenbcrg— riRid conseivativo as lie was in theology — openly
cbnllengwi it ; and since then it has been controverted at length ia
Noldeke's Bsilrayt air Kenntniss iler Pon-Ie dir alien Aruber (Han-
over, 1864), p. xvii. sqq. Our highest authority on Arabic poelry,
Professor Ablwonlt, concurs in (Ids conclusion ; see his BeiitcrkuiirieH
iliicr did .U-c!ilheil fill- itllni •imbischen OaliclUc (1S72), p. 25 .tj.
* The possugo is cited by Noldeke, SeitrUyt:, p. xx. jq.
M O'A L L A K A T
537
liimself coiTDctly, they also called this modified collection
Mo'allalcdt. Mofaddal employs, besides, the names "the
seven long [poems] " and " the necklaces." ITiis last be-
came afterwards a common title for the seven poems.
The comparison of songs to strings of pearls is a very apt
one, from the nature of the Arabic poem, composed as it
is of separate loosely-comiected parts. Hence it became
ao popular that even in ordinary prose to speak in rhyth-
ini<al form is called simply nazTn, "to string pearls."
Mofaddal expressly opposes the view of those who did not
acknowledge the pre-eminence of the seven poets selected
by him. This appears to be an attack on Hammid for
including in his collection the works of two men who for
poetic fame could certainly never enter the lists with
Nibigha and A'shiL It is prima facie rndre likely that a
later writer should have replaced the less- famous poets by
those who were universally placed in the first rank, than
vice versa. Perhaps another fact is of some importance
here, Hammid, a Persian by descent, was a client of the
Arab tribe, Bakr ibn WiiL In the heathen period this
tribe was much at war with the closely -related tribe
Taghlib. Now of all Arabic poems none was more famous
thaa that in which 'Atnr ibn Eolthiim celebrates in
glowing terms the praises of his tribe Taghlib. If,
therefore, Hammid's collection embraced this poem, it was
very natural for bim to gratify his patrons the Bakrites
by placing alongside of it that of Hirith — a Bakrite and
contemporary of "Amr — ^where he extols his own tribe and
assails the Taghlibites with bitter scorn. Such considera-
tions did not affect Abi!i 'Obaida and MofaddaL
The authority of these men has so for prevailed that
the poems of their favourites Kdbigha and A'shi often
appear in the manuscripts, not indeed instead of those of
'Antara and H&rith, but after the other seven. Thus we
sometimes read of nine Mo'allakit. The first author in
whom the writer has observed this is the great philosophic
historian Ibn Khaldi^ (a.d. 1332-1406) ; he mentions
instead of Hirith the far more celebrated 'Alkama;
whether relying on ancient authority, or by an oversight,
we cannot telL In an excellent collection of forty-nine
long poems by Abii Zaid al-Korashi (date unknown)
Mofaddal's seven poets appear in the first class, "the
necklaces; " but Ndbigha and A'shi are each represented
by a different piece from that usually reckoned among the
Mo'allakit. By this editor the name "golden poems,"
which, as we have seen, sometimes occurs as a synonym of
" Mo'allakit," is applied to seven quite distinct songs.^
This imcertainty as to the selection and the titles may
serve as an additional proof that the " suspension," on the
Ealia or anywhere else, is a fable.
The lives of these seven (or nine) poets were spread
over a period of more than a himdred years. The earliest
of them, according to the common and probably correct
opinion, was Amp.aalkais (pronounced also Imroolkais,
liuraalkais, &c.), regarded by many as the most illustrious
of Arabian poets. His exact date cannot be determined ;
but probably the best part of his career fell within the
first half of the 6th century. He was a scion of the royal
house of the tribe Kinda, which lost all its power at the
death of King HArith ibn 'Amr in the year 529.^ The
poet's royal father, Hojr, by some accounts a son of this
Hiirith, was killed by Bedouins. The son led an adven-
turous life as a refugee, now with one tribe, now with
another, and appears to have died young. The anecdotes
related of him — which, however, are very untrustworthy
in detail — as well as his poems, imply that the glorious
' See Noldel^e, Bdtriige, p. xxi., asd the catalogue of the Arabic
codd. in the British Museum, p. 480 sqq.
" See Tnhari's Geschichti dtr Ptrier and Araiivr ^ y t,Ji>eT»etst von
n. mideke (Lejden, 1879), p. 171.
memory of his house and the hatred it inspired were still
comparatively fresh, and therefore recent.
The Mo'ailaka of 'Amr hurls defiance against the king
of Hlra, 'Amr son of Mundhir, who reigned from the
summer of 554 till 568 or 569, and was afterwards slain
by our poet.' This prince is also addressed by HiEiTH in
bis Mo'allaka. Of Tabafa, who is said to have attained
no great age, a few satirical verses have been preserved,
directed against this same king. This agrees with the
fact that a grandson of the Kais ibn EMlid, mentioned as
a rich and influential man in T^rafa's Mo'allaka (v. 80 or
81), figured at the time of the battle of Dhii Kir, in which
the tribe Bakr routed a Persian army. This battle falls
between a.d. 604 and 610 (Noldeke's Tabari, p. 311).
The Mo'allaka of 'Antara and that of Zohaib contain
allusions to the feuds of the kindred tiibes 'Abs and
Dhobyin. Famous as these contests were, their time cannot
be ascertained. But the date of the two poets can be appmxi-
mately determined from other data. Ka'b, son of ZoLair,
composed first a satire, and then, in the year 630, a eulogyi
on the Prophet ; another son, Bojair, had begun, some-
what sooner, to celebrate . Mohammed. 'Antara killed the
grandfather of the Aljnaf ibn Kais who died at an advanced
age in A.D. 686 or 637 ; he outlived 'Abdallih ibn Simma,
whose brother Doraid was a very old man when he fell in
battle against the Prophet (early in a.d. 630) ; and he had
communications with AVard, whose son, the poet 'Orwa, may
perhaps have survived the flight of Mohammed to Medina.'
From all these indications we may place the productive
period of both poets in the end of the 6th century.* The
historical background of 'Antara's Mo'allaka seems to lie
somewhat earlier than that of Zohair's.
To the same period appears to belong the poem of
'Alkama, which, as we have seen, Ibn Khaldiin reckons
amongst the Mo'allalfit. This too is certainly the date
of NAbigha, who was one of the most distinguished of
Arabic poets. For in the poem often reckoned as a
Mo'allaka, as in many others, he addresses himself to the
above-named No'min, king of Hira, who reigned in the
two last decades of the 6th century. The same king is
mentioned as a contemporary in one of 'Alkama's poems.
The poem of A'sai, which Mofaddal placed among the
Mo'aUakit, contains an allusion to the battle of Dhii Kar
(under the name "Battle of Hinw," v. 62). This poet,
not less famous than Nibigha, lived to compose a poem
in honour of Mohammed, and died not long before a.d.
630.
LabId is the only one of these poets who embraced Islam.
His Mo'allal?a, however, like almost all his other poetical
works, belongs to the pagan period. He is said to have
lived till 661 or even later ; certainly it is true of fiini,
what is asserted with less likelihood of several others of
these poets, that he lived to a ripe old age.
We have already mentioned that the old Arabic poetry
was transmitted not by manuscripts but simply through
oral tradition. Many pieces, especially the shorter ones,
may have owed their preservation to their hold on the
popular memory. But, fortunately, there was a class of
men who made it their special business to learn by rote,
and repeat, the works either of a single poet or of several.
The poets themselves used the services of such rhapso-
dists {rdwU). The last representative of this class is
Hammid, the man who formed the collection of Mo'alla-
kit ; but he, at the same time, marks the transition from
» See Noldeke's Talari, pp. 170, 172.
* This evidence might bo supplemented from a poem in Zohair's
name, whose author describes himself as a man of ninety yeara, and
in which the downfall of King No'mdn of Hira (a.d. 601, eee fahxrl,
p. 347) is spoken of as a not very recent event. Bnt the geruiuenesj
of this poem is moio than doubtful (see Alihvordt, op. ciU pi 64i and C.
J. liyaU in the Academy, March 13, 18S0, p. 192).
:o~;-u*
538
M 0 A L L A K A T
the rhapsodist to the critic and scholar. Now, when we
consider that more thaii a century — in some cases two
centuries — elapsed before the poems were fixed by literary
men, we must be prepared to find that they have not
retained their original form unaltered. The most favour-
able opinion of the rhapsodista would require us to make
allowance for occasional mistakes ; expressions would be
interchanged, the order of verses disarranged, passages
omitted, and probably portions of different poems pieced
together. The loose structure of the ancient poeras ren-
dered them peculiarly liable to corruptions of this kind.
But the fact is that Hamm4d in particular dealt in the_
most arbitrary fashion with the enormous quantity of
poetry which he professed to know thoroughly. He is
even charged with falsifications of all sorts in this depart-
ment. Of others, again — and notably of the great philolo-
gist Ivhalaf, " the Eed " — it is credibly reported that they
used their intimate knowledge of the style and langiiage
of the ancients to^pass off whole poems of their own
making as the productions of earlier authors. The worst
anticipations are ordy too completely confirmed by an
examination of such pieces as are still preserved, as is
shown mbst conclusively in AhJ wardt's Bemerhungen, already
cited. The seven Mo'allakAt are indeed free from the sus-
picion of forgery, but even in them verses are frequently
transposed ; ir. all there are lacunae ; and probably all
contain verses which do not belong to them. Some of
them have more than one introduction. This is the case
even with the poem of 'Amr, although, as the finest pane-
gj-ric of his very powerful tribe, it must have had a wide
circulation. The true introduction begins at v. 9 ; before
that we find another which certainly does not belong to
this poem, and can hardly be the work of the same poet.
"Amr lived in the desert' regions near the lower Euphrates,
under the Persian dominion ; whereas the author of v. 8
boasts of his carousals in several parts of Boman Syria,
and in v. 1 he speaks of drinking wine from a place in
Northern Syria. It is evident that all attempts to restore
the original order, to fill up blanks, or to remove interpola-
tions, can only be carried to a certain degree of probability
at the best ; there must always be a large subjective ele-
ment in judgments on points of the kind. Still less can
we hope to discover and rectify the minor changes, in single
t.\[>ressions or grammatical forms, which the text may have
undergone before it was fixed in writing. It may be re-
marked in this connexion that where any ancient song has
been transmitted through two different grammatical schools
it generally ai:^ear3 in two considerably divergent forms,
each having been taken down from the lips of a separate
rAwt Of secondary importance are the errors due to
later copyists. Considerable as these often are, we are, at
least in many cases, better able to correct them.
Even the masters of old Arabian poetry do not exhibit
Kuch characteristic differences in their general manner and
B'jyle as to leave in the mind a clear idea of their indivi-
duality. A few distinct poetic types emerge, but the great
'majority of these poets present a somewhat monotonous
aspect to the Western scholar, who indeed can at best have
but a very imperfect feeling for nuances of style in this field.
But if we are thus unable to isolate the various constituent
parts of this ])oetical literature, and pass a critical opinion
on each, we do get from this literature, as a whole, what
is of far greater importance than an iesthetic estimate of
this or that particular poet, viz. a poetic picture of the
whole life and activity of that remarkable people which,
amid the endless agitation and endless sameness of its
existence, and in an extremely inhospitable region, was
'rej)aring one of the mightiest revolutions in the history
pi the world. This collective impression is hardly impaired
by the iuvoluiitarv alterations made by the rdwis ; nor is
it greatly distorted by the forgers of the 2d century of
Islam, who were thoroughly familiar with the spirit and
style of antiquity, and seldom did violence to them.
The critics of the 2d and 3d centuries a.h. tinani-
mously ranked the poets of the heathen period abova
those of Islam ; and in that verdict we must concur. The
older Moslem poets were for the most part mere Epigoni,
content, for better or worse, to borrow the style of their
pagan predecessors. It is only natural, therefore, that tha
seven best poems should have been selected from the pro
ductions of heathenism. But how these particiilar seven
came to be fixed upon, it is difficult to decide. It is
remarkable that people who knew thousands of such poems
should have agreed as to the superiority of five, and only|
differed about two. No doubt the selection was greatly
influenced by the widely-established reputation of certain
poets, like AmraaUjais, Zohair, and Tarafa ; while in other
cases single poems, such as that of 'Ami-, stood in high
repute for special reasons. Still, even we, with a much
narrower range of selection, should hardl}' pick out these
seven as the finest. In all probability our choice would
not light on a single one of them. The truth is, our
esthetic ideal is essentially different from that of those
old litterateurs. And, while we may certainly consider our
own taste, formed on the model of the Greeks and the best
of the modems, to be on the whole purer than theirs, we'
must not forget that they had the advantage of perfect
knowledge of the language and the subject-matter, and
could thus perceive a multitude of beautiful and delicato
touches, which we either miss entirely or realize with labo-
rious effort. The world of the old Arabian poet lay at an
infinite remove from ours. His mental horizon was narrow ;
but within that horizon every minute detail was seized
and designated with precision. Among the nomads, for
example, the smallest point of the horse or camel that
the eye can see has its importance ; the language has pre-
cise and generally understood words for them all, where
ours has only technical terms. It is the same with all the
physical properties of the animal — its paces, etc. Thu.s,
when a poet faithfully described the exterior and the
deportment of his camel, that was to his hearers — and tha
same is true of later critics — a genuine pleasure, because
the description conveyed to them a definite pictorial im-
pression. But we do not understand the details of the
picture ; or, when at best with all the resources of tradition
and natural history we have gained some tolerable compre-
hension of them, the whole still leaves us indifferent. A
camel to us is simply not a poetical object ; and even a
horse ceases to be SEsthetically interesting— except perhaps
to a sportsman — when one is asked to go over his points
in detail. For this reason we are apt to find a great part
of Tarafa's Mo'allalja, and many parts of the poems of
Amraalljais, viewed as poetry, distasteful rather than
interesting. More attractive are the descriptions of tha
life and habits of wild animab in the desert, such as tha
wild ass and some species of antelope, which the poets are
fond of introducing (see, e.g., the Mo'aUaVa of Labld).
Theie are also many vivid sketches from nature to be mot
with, — nature, of course, as seen in the very monotonous
Arabian landscape. Monotony, indeed, is a predominant
characteristic of this poetry, ^yhen one first reads poems
where the bard begins by shedding tears over the scarcely
perceptible traces of the dwelling of his beloved in years
gone by, one's sympathy is aroused. But when poem after
poem is found to commence with the same scene, and pos-
sibly with almost the same words, the emotion is somewhat
damped. No doubt such occurrences must really have
been very common in the nomad life ; nevertheless the
suspicion becomes at last irresistible that for the moet
part all this is piure fiction. Nor can we be surn thai tl>«
M OB — M O B
539
poets are always to be taken au terieux when they describe
those carousals, and other adventures in peace and war, of
which they Ioto to boast. They are probably more serious
in the narratives of their love experiences : these are often
very highly coloured, and yet are always pervaded by a
certain natural refinement, which is too often wanting in the
later erotic poetry of the Moslems. But there, too, our enjoy-
ment is frequently marred by minute and even prosy de-
scriptions of the physical charms of the object of affection.
The lyrical and even the more rhetorical passages of the
poems make in general a deeper impression upon us than
the descriptive portions, to which they owe their distinctive
character, and which are often intimately blended with the
former. When those old Arabs are really moved by love,
or rage, or grief, when personal or tribal vanity vents itself
in immoderate boasting, invective, or banter, then they
strike chorda that thnll our breasts. In those passages
where genuine human feeling is stirred, they also display
far greater individuality than in the more conventional
descriptions. Especially affecting are the numerous pass-
ages or complete poems which mourn over the beloved
and venerated dead. Their sober practical philosophy too,
as it is presented in the Mo'allaka of Zohair and in many
of Labfd's poems, is really impressive.
The Mo'allak^t are highly characteristic specimens of this
poetry. They exhibit nearly all its merits as well as most
of its defects. Amongst its merits we ought, perhaps, to
include the unfailing regularity of the verse. That a people
living under such extremely simple conditions should have
cultivated a purely quantitative metre, so euphonious and
so rigorously adhered to, is a fact worthy of our highest
admiration: It is one evidence of that sense of measure
and fixed form which is, in other directions also, a marked
feature in the life and speech of the Arabs. The mere fact
that in their verses they give so much attention to elegance
of expression deserves commendation. Amongst the defects
of this poetry we must emphasize the loose connexion
between the separate parts. We require a poem, like any
other work of art, to be a compact unity ; the Arabs and
many other Orientals lay all the stress on the detaOs. In
the Mo'allaka of Tarafa, for instance, after the poet has
spoken long enough about his beloved, he starts off in this
fashion : " But I banish care when it comes near with a " —
she-camel of such and such qualities, and then proceeds
to give a description of his riding-cameL Equally abrupt
transitions occur in almost all these poems, gener^y more
than once in the same poem. In many cases a sort of unity
is preserved by making the different sections represent so
many scenes from the life of the poet or from the common
life of the Bedouins; but even then there is something
unsatisfactory in the want of real connexion. It does not
mend matters much when the poet keeps up a merely
mechanical transition ; as, for example, when he speaks
first of his camel, then with the words "it is as swift as a
wild ass which," <fcc., passes to a description of that unimnl^
and again proceeds, " or as swift as an ostrich which," (tc^
in order to introduce the ostrich.
This loose structiwe of the poems explains the fact that
from a very early period particular pieces were culled from
larger works and recited by themselves. For the town-
Arabs of later times this procedure was especially convenient.
For them the wild ass or oryx-antelope had little attraction ;
and on the camel they bestowed about as much notice as
' we do on our dray-horses and waggons. But the love and
hate, the pride and scorn, the fierce lust of revenge and the
wailing grief, the bravery and the gaiety, which breathed
through the old Bedouin songs, had an inten.se fascination
for them. We see that their attitude towards that poetry
had in some degree approximated to our own. Hence it is
that some ant.holoeies from the old poetry.- made by men
of learning and ability, with an eye to contemporary tastes,
are on the whole much more pleasing to us than the com-
plete poems themselves. This is eminently true of the
excellent collection edited by Abfi Tammim, himself a con-
siderable poet (first half of the 9th century), under the
title " Hamisa " (Valour). This collection, which, however,
embraces many pieces of the Moslem period, is certainly
fitted to give a European a rather too favourable idea of
ancient Arabic poetry. Whoever wishes really to know
that poetry — and without this knowledge it is impossible
to understand the Arabs themselves or their language-
must betake himself to those which, like the Mo'aUakAt and
others, have been preserved more or less in their integrity.
The Mo'allakat have been repeatedly printed, separately and
coUectivcly, both in the West and the East, generally with ao
Arabic commentary. A good commentary by a competent European
is a real desideratum. A work of this kind would do more for ths
understanding of the poems than any poetical translation, which
must always fail in rendering these definite concrete expressions of
the Arabs for which we possess neither the idea nor the image. A
translation must either De a mere paraphrase or else substitute some-
thing utterly vagiie. (TH. N.)
MOBILE, a city and port of entry of the United States,
the capital of Mobile county, and, though not the capital,
the largest city of Alabama, lies 140 miles east of New
Orleans, on a sandy plain on the west bank of Mobile
river, one of the arms of the Alabama. The municipal
boundary includes an area about 6 miles long by 2
or 3 in breadth ; but, excluding the suburban villas
scattered about the nearer hills, the portion occupied by
the buildings of the city proper is not more than a mile
square. In the matter of paving and shade the streets
are generally good, and Government Street especially,
with its fine oak trees and gardens, forms an attractive
promenade. Besides the spacious granite building erected
in 1859 to accommodate the Custom-House, the Post Office,
and the" United States courts, the principal edifices are the
Roman Catholic cathedral of the Immaculate Conception
(1833), Christ Church (Episcopal) (1837), the City Hos-
pital (1830), the United States Marine Hospital (1836),
the Providence Infirmary, the conjoint market-house and
municipal buildings. Barton Academy (occupied by the
high schools), and the Alabama Medical CoUege (founded
in 1859). About 6 miles out, at Spring Hill, is the
Jesuit College of St Joseph, established by Bishop Portier
in 1832. As a commercial centre Mobile is in some re-
spects very favourably situated. It is the only port of
Alabama ; the estuary on which it stands is the outlet for
several navigable rivers ; and it is the seaward terminus
of the MobUe and Ohio railroad, the Mobile and Mont-
gomery, and the Grand Tnmk. But, on the other hand,
it lies 25 miles from the coast ; the lagoon-like bay cut
off from the Gulf of Mexico by the narrow isthmus of
Mobile Point is extremely shallow; and in 1879 no vessel
drawing more than 13 feet could load and unload in
the harbour with safety. Since 1827, it is true, various
works have been undertaken to improve the approaches :
the Choctaw Pass and the Dog River Bar, which had
formerly a depth of little more than 5 and 8 feet
respectively, were deepened to 17 feet by 1882 ; but
Mobile will not take rank as a satisfactory ocean port tiQ
the scheme (now in operation) for constructing a wido
channel more than 20 feet deep right through the bay has
been fully carried out. The cost 6f the necessary works
being beyond the power both of the city and State, Con-
gress has granted §270,000 for the purpose of widening
the channel to 200 feet, and deepening it to 23 feet. ^ A
private company, established in 1876, has built a break-
water in the bay, and greatly increased the safety of the
harbour. For the years between 1855 and 1859 the
average value of exports and imports was respectivejy
540
M O E-
.■523,419,266 and 6711,420 ; the following figures for recent
vears show a considerable decline on the total ; — -
Years ending in
Exports.
Imports.
1877
1878
1879
1880
ISSl
1882
$12,784,171
9,493,306
6,219,818
7,188,740
6,S95,140
3,258,605
$648,404
1,148,442
644,628
425,519
671,252
396,573
In cotton, ■which forms the staple export, the falling off is par-
ticularly noticeable, 632,308 bales being the average for 1855 to
1859, and 365,945, 392,319, and 205,040 bales the qu-intities for
1879, 1880, and 1831. A great deal of what comes to the Mobile
market is sent to New Orleans for shipment, partly that it may
ohtain a higher piico as " Orleans " cotton. Lumber shingles,
turpentine and rosin, fish and oysters, and coal, are also important
items, but do not mate in the aggi'egato so much as half the value
nf the cotton. Among the local industrial establishments are
pcrcral spinning-mills, breweries, cooperages, shipbuilding yards,
Ibuudries, and sash and door works. The market gardeners of the
outsldrts produce a large quantity of cabbages, potatoes, water-
jiielons, tomatoes, &c., to supply the cities of the western and
northern States (value in 1879, §112,620; 1880, $174,483; ISSl,
S159.706; 1382, $367,194; 1883, estimated $700,000). Though
iu 1820 it had no more tlian 2672 inhabitants. Mobile had 31,255
in 1880 ; the figmes for the intermediate decades being 3194 (1630),
12,672 (1840), 20,515 (1850), 29,258 (1860), and 32,034 (1370).
Founded as a foi-t by Lemoyne d'Ibervillo (de Bienville) in 1702,
^Mobile continued to be the capital of the colony of Louisiana till
1723, when this rank was ti'ansfeiTed to New Orleans. The site
selected- by Lemoyne was probably about 20 miles above the pre-
sent position, which was iii-st occupied after the 'floods of 1711.
By the Treaty of Paris, 1763, Mobile and part of Louisiana were
ceded to Britain ; but in 1780 the fort (uow Fort Charlotte) was
captured by the Spanish general Galvez, and in 1783 it was recog-
nized as Spanish along Avith other British possessions on the Gulf
of Mexico. General Wilkinson, ex-governor of Louisiana, recovered
the tou-n for Louisiana in 1813, and in 1819, though its population
did not exceed 2500, it was incoriwrated as a city, m 1864-65
Mobile and the ueighboui-hood was the scene of important military
and naval engagements. The Confederates had suiTounded the city
by three lines of defensive works, but the defeat of their fleet by
.•\drairal Farragut, and the capture of Fort ilorgan, Spanish Fort,
iind Fort Blakelly, led to its immediate evacuation. As a municipal
corporation, ilobile had got into such financial difficulties by 1879
Ihat its cil^ charter was rejKjaled, and a board of commissioners
. stahlished for the liquidation of its debt of $2,497,856.
MOBIUS, August Ferdinand (1790-1868), astronomer
and mathematician, was born at Schulpforta, November
17, 1790. At Leipsic, Gottingen, and Halle he studied
for four years, ultimately devoting him.self to mathematics
and astronomy. In 1815 he settled at Leipsic as privat-
docent, and the next year became e.-ctraordinary professor
of astronomy in connexion with the university. Later
ho was chosen director of the university observatory,
which wa3 erected (1818-21) under his superintendence.
In 1844 he was elected ordinary professor of higher
mechanics and astronomy, a position wliich he held till
his death, September 26, 1868. His doctor's dissertation,
De compuiandis occuHationibus fixafum ;;£7' planetas
(Leipsic, 1815), established his reputation as a theoretical
astronomer. Die Hauptsiitze der Astronoinie (1S36), Die.
Elemente der ilechanik des llimmds (1843), may be noted
amongst his other purely astronomical publications. Of
more general interest, however, are his labours in pure
mathematics, which appear for the most part in Crelle's
Journal from 1828 to 1858. These papers are chiefly
geometrical, many of them, being developments and appli-
cations of the methods laid down in his great work, Dcr
£arycentnsche Calcul (Leipsic, 1827), which, as the name
implies, is based upon the properties of the mean point or
centre of mass. Any point in a plane (or in space) can be
represented as the mean point of threo (or four) fixed
points by giving to these proper weights or coefficients, —
an obvious principle which leads in the hands of Miibius
to what no doubt is the chief novel feature of the work, a
■■:.i o G
system of homogeneous coordinates. Besides this, how-
ever, the work abounds in suggestions and foreshado'n'ings
of some of the most striking discoveries in more recent
times — such, for example, as are contained in Grassmann's
Ausdehnungslehre and Hamilton's Quaternions. He must
be regarded as one of the leaders in the introduction of
the powerful methods of modem geometry that have been
developed so extensively of late by Von Standt. Cremona, '
and others.
MOCHA, a town of Yemen on the coast of the Red Sea,
in E. long. 43° 20', N. kt. 13° 19'. The point of the coast
where MochA lies appears to have owed early import-
ance to its good anchorage, for the Muza of the Petiplvs
{Geoj. Gr. Min., i. 273 sqq.), a great seat of the Red Sea
trade in antiquity, seems to be identical with the modem'
Miiza" (Yiki'it, iv. 680; Niebuhr, Desc. de VArahie, p. 195),
a few miles inland from Moch.i. Mochi itself is a modem
to%vn, which rose with the coffee trade into short-lived pros-
perity. The French expedition of 1709 found it a place of
some 10,000 inhabitants, and its importance had increa.sed
half a century later, when Niebuhr visited it. The chief
trade was then with British India. Lord Valencia in 1 806
still found the town to present an imposing aspect, with its
two castles, minarets, and lofty buildings ; but the popula-
tion had sunk to 5000. ' The internal disorders of Arabia
and the effoi-ts of Mohammed Ali to make the coffee trade
again pas.s through India accelerated its fall, and the place
is now a mere village. Mochi never produced cofTee, and
lies indeed in a quite sterile plain ; the European name of
Jlochi coffee is derived from the shipment of coffee there.
The patron saint. Sheikh Shadali, was, according to legend,
the founder of the city and father of the coffee trade.
MOCKING-BIRD, or Mock-Bikd (as Charleton, Ray,
and Catesby wrote its name), the Mimus polyglottvs of
modern ornithologists, and the well-known representative
of an American group of birds usually placed among the
Thrushes (?.».), Turdids, though often regarded as
forming a distinct section of that Family, differing by
having the tarsus scutellate in front, while the tj'pical
Thrushes have it covered by a single horny plate. The
Mocking-bird inhabits the gi'eater part of the United
States, being In the north only a summer-visitant ; but,
though breeding yearly in New England, is not common
there, and migrates to the south iii A\-intcr, passing that
season in the Gulf States and Mexico. It appears to be less
nimierous on the western side of the Alleghanies, though
found in suitable localities across the continent to the
Pacific coast, but not farther northward than Wisconsin,
and it is said to be common in Kan.sas. Audubon states
that the Mocking-birds wliich are resident all the year round
in Louisiana attack their travelled brethren on the return
of the latter from the north in autumn. The nafncs of
the species, both English and scientific, have been bestowed
from its capacity of successfully imitating the cry of many
other birds, to say nothing of other sounds, in addition to
uttering notes of its OAvn whi.h possess a varied range and
liquid fulness of tone that are unequalled, according, to its
adinircrs, even by those of the NicnTiNG.^LE (y.t'.). This
opinion may perhaps be correct ; but, from the nature
of the case, a satisfactory judgment can scarcely be pro
nounced, since a comparison of the voice of the U\-
songsters can only be made from memory, and that is (li
course affected by associations of ideas which would i)rc-
clude a fair estimate. To hear either bird at its best it
must bo at liberty ; and the bringing together of cajitive
examples, unless it could be done with so many of each
species as to ensure an honest trial, would be of little avail.
Plain in plumage, being greyish-brown above and dull
white below, while its quills arc dingy Id.ick, vaiicgated
with white, there is little about the Mocking-birds appear-,
MD^D — M O D
541
anco beyond its graceful form to recommend it ; but the
lively gesticulations it exhibits are very attractive, and
therein its European rival in melody is far surpassed, for
the cock-bird mounts aloft in rapid circling flight, and,
alighting on a conspicuous perch, pours forth his ever-
changing song to the delight of all listeners ; while his
actions in attendance on his mate are playfully demonstra^
tive and equaUy interest the observer. The Mocking-bird
is moreover of familiar habits, haunting the neighbourhood
of houses, and is therefore a general favourite. The nest
is placed with little regard to concealment, and is not dis-
tinguished by much care in its construction. The eggs,
from three to six in number, are of a pale bluish-green,
blotched and spotted with light yellowish-brown. They,
as well as the young, are much sought after by snakes, but
the parents are often successfvd in repelling these deadly
enemies, and are always ready to wage war against any
intruder on their precincts, be it man, cat, or hawk. Their
food is various, consisting of berries, seeds, and insects.
Some twelve or fourteen other species of ilimus have been recog-
nized, mostly from South America ; but M. orpheua seems to be
common to some of the Greater Antilles, and if. hilli is peculiar to
Jamaica, while the Bahamas have a local race in M. haJuniunsis.
The so-called Mountain Mocking-bird (Orcoscoptcs vwntanus) is a
form not very distant from Mimiis; bat, according to Mr. Eidgway,
it inhabits exclusively the plains overgrown with ArUmisia of the
interior tableland of North America, and is not at all imitative in
its notes, so that it is an instance of a misnomer. Of the various
other genera allied to Mimiis, those known in the United States as
Threshers, and belonging to the genus Harporhynchua — of which
sir or eight species are found in North America, and are very
Thrush-Uke in their habits — must be mentioned ; but there is only
room here to dwell on the Cat-bird {Oaleoscoptea caroUnensis)^ which
is nearly as accomplished an imitator of sounds as its more ccle-
htated relative, with at the same time peculiar notes of its orni,
from one of which it has gained its popular name. The sooty -gi'ey
colour tha», deepening mto blackisn-brown on the crown and
quills, pervades the whole of its plumage — the lower tail-coverts,
which are of a deep chestnut, excepted — renders it a conspicuous
object ; and though, for some reason or other, far from being a
favourite, it is always willing when undisturbed to become Ultimate
with men's abodes. It has a much wider range on the American
coutuient than the Mocking-bird, and is one of the few sjiccies that
are resident in Bermuda, while on more than one occasion it is
s-tid to have aitpeared iu Eui'ope.
■ The name liocking-bud, or more frequently Mock-Nightingale,
is iu Eugland occasionally given to some of the Wattle ns (q.v.),
especially the Blackcap (Sylvia airicapiUa), and the Sedge-binl
{Acrocijihalxts schanobxnuft). In India and Australia the same
uame is sometimes applied to other species. (A. N. )
1I0DEN.\, one of the principal cities of Northern Italy,
formerly the capital of a duchy, and still the chief town
of a province and the seat of an archbishop, is situated in
the open country in the south side of the valley of the Po,
lietween the Secchia to the west and the Panaro to the east.
By rail it is 31 miles E.S.E. of Parma, 24 W.N.W. of
I'.ologna, and 37 S. of Mantua. The observatory stands
135 feet above the level of the sea, in 44° 38' 52" N. lat.
and 10° 55' 42' E. long. Dismantled since 1816, and now
hirgely converted into promenades, the fortifications still
;,'ive the city an irregular pentagonal contour, modified at
the north-west corner by the addition of a citadel also penta-
gonal Within this circuit there are various open areas —
the spacious Piazza d'Armi in front of the citadel, the
public gardens in the north-east of the city, the Piazza
Grande in front of the cathedral, arid the Piazza Reale to
the south of the jjalace. The .Smilian Way crosses obliquely
right through the heart of the city, from the Bologna Gate in
the east to that of Sant' Agostino in the west. Commenced
'by the countess Matilda in 1099, after the designs of
Lanfranc, and consecrated in 1184, the cathedral (St
Geminian's) is a low but handsome building, with a lofty
crypt, three eastern apses, and a fajade still preserving some
rtlrioua sculptures of the 12th and 15th centuries. The
bell-tower, named La Ghirlandina from the bronze garland
surrounding the weathercock, is lined with white marble.
and is 315 feet high; in the basement may be seen the
wooden bucket captured by the Modenese from the Bo-
lognese in the afeay at Zappolino (1325), and rendered
famous by Tassoni's Secchia Sapita. Of the other churches
in Modena, San Pietro has terra^cottas by the local artist
BegareUi, and S. Agostino (now S. Michele) contains the
tomb of Sigonius and the tombstone of Mmatori. The old
ducal palace, begun by Duke Francis I. in 1635 from the
designs of Avanzini, and finished by Francis Ferdinand V.,
is an extensive marble building, and now contains the
library {Bib. Pcdatina, see vol xiv. p. 530), picture-gallery,
and museum. Many of the best pictures in the ducal
collection were sold in the 18th century, and found their
way to Dresden. The valuable Mmeo Lapidario in a
buUding near Porta Sant' Agostino is well known to the
1. Moseo Lapldarla I
2. 8. Agostino. 1
3. Aoademy of Fin* Arts. |
Plan of Modeuo.
ft Doineuieo. I 7. CftthedraL
Royal PaUee. 8. Campanile GhirlADdiBa.
. AichbiBhop's Palace. | 0. Uuivenity.
la 8. Hetro.
classical antiquary through Cavedoni's Dichiaraiione dtgli
antichi marmi Moderuti (1828), and the supplements in the
Memairt of the Academy, vol it, &c The university of
Modena, originally founded in 1683 by Fiancis 11., is
mainly a medical and legal school, but has also a faculty
of physical and mathematical science. It has about
twenty-five professors, and from 200 to 250 students ; a
library of 20,000 volumes, an observatory, botanical gar-
dens, an ethnographical museum, ic. The old academy
of the Dissonanti, dating from 1684, was restored by
Francis in 1814, and now forms the flourishing Eoyal
Academy of Science and Art {Memoin since 1833) ; and
there are besides in the city an Italian Society of Science
founded by Anton Mario Lorgna, an academy of fine
arts, a military college (1859), an important agricultural
college, and a lyceum and gymnasium, both named after
Miu^tori. In industrial enterprise the Modenese show but
little activity, silk and linen goods and iron-wares being
almost the only products of any note. Commerce i.-<
stimulated by a good position in the railway system, and
by a canal which opens a water-way by the Panaro and
the Po to the Adriatic. The population of the city was
32,248 in 1861, and 30,854 in 1871 ; that of the com-
mune 55,512 in 1861, and 58,058 in 1881.
The Duchy of Modena, an independent sovereign stata
542
M O D — M 0 F
(1452 to 1859), ultimately extended from the Po tc the
Mediterranean, and was bounded N. by Locibardy and the
Papal States, E. by the Papal States and Tuscany, S. by
Tuscany, Sardinia, and the Mediterranean, and W. by
Sardinia and the duchy of Parma, Its greatest length,
from Porto -Vecchio, on its northern frontier towards Man-
tua, to the outlet of the Pannigncla torrent, on the Sardinian
frTjntier, was Sii miles ; and its greatest width, from the
pass of Calama, on the Papal and Tuscan frontier, to the
right bank o£ the Enza, on the frontier of Parma, was 37
miles. The area fas 2371 square miles, of which three-
fifths were mountainous. In ISoo the population was
606^159. The duchy had six provinces — Modena, Reggio,
GuastaUa, Frignano, Garfagnana, Massa-Carrara.
Kodena is the ancient Mutina, which was annexetl by the Romans
tloag with the rest of the territory of the Boii. In 1 S3 b. c. Mntina
became the seat of a Roman colony. During the civil wa:-s Marcus
Brutns held oat within its walls against Pompei'ds in 78 B.C., and
in H B.O. the place was defended by D. Bmtns against M. Antony.
The 4th centiuy fonnd Matina in a state of dec^y ; the ravages of
Attila and the tronbles of the Lombard period left it a min£d city
in a wasted land. In the 8th century its exiles founded, at a dis-
tance of 4 miles to the north-west, a new city, Citti Geminiana (still
represented by the village of Cittanova) ; bat about the close of
the 9th century Modena was restored and refort^ed by its bishop,
Laedoinus. When it began to build its cathedral (1099 A.D.) the
dty was part of the possessions of the countess Matilda of Tuscany :
bat when, in 1184, the edifice was consecrated by Lucius III., it
was a fiee community. In the wars between Frederick IL and
Gregory IX it sided with the emperor, though ultimately the papal
party was strong enough to introduce confusion into its poUcy. . In
1288 Obizzo d'Este was recognized as lord of the city ; after tbe
death of his successor, Azzo VIII. (1308), it resumed its communal
independence ; but by 1336 the Este femily was again in power.
Constituted a duchy in 1452 in favour of Borso d'Este, and emargcd
and strengthened by Hei-cules II., it became the ducal residence on
the incorporation of Ferrara with the States of the Church (1593).
Francis L (1629-1658) erected the citadel and commenced the palace,
which was largely embellished by Francis II. Rinaldo (ob. 1737)
was twice driven from his city by French invasion. To Francis III.
{1698-1780} the city was indebted for many of its pubUc buildings.
Hercules III. (1727-1803) saw his states transformed by the French
into the Cispadine RepubUc, and, having refused the principaUty
of Breisgau and Ortenau, offered him in oompensation by the treaty
of Campo Formio, died an exile at Treviso. H is only daughter, Maria
Beatrice, married Ferdinand of Austria (son of Maria Theresa), and
in 1814 their eldest son, Ferdinand, received back the Slati Estoisi.
TTiq rule was subservient to Austria, reactionary, and despotic. On
the outbreak of the French Revolution of 1830,Francis IV.seemed for
a time disposed to encourage the corresponding moveLient in Modena;
but no sooner had the Austrian army put an end to the insurrection
in Central Italy than he returned to his prerious poHcy. Francis
Ferdinand V., who succeeded in 1846, followed m the main his
bther's example. Obhged to leave the city in 1S48. h3 was restored
by the Austrians in 1349 ; ten years later, on 20th August 1853,
the representatives of the Modenese, under the direction of Carlo
Farini, declared their territory part of the kingdom of Italy, and
their decision was confirmed by the plebiscite of 1S60.
Natives of Modena are Fallopius the anatomist, Tarquinia
Uolza, Sadoletius, Sigonius, Tassoni, and Cavedoni the archreologist ;
the names of Zatcana, Tiraboschi, and Mnratori are associated with
its library. Tiraboschi's Bibliothica Jtfodtncnsis, 6 vols., contains
an account of all the literary personages of the duchy.
Sco Vedriani, Storia d( Modcr.rnj 1666 ; "nraboschi, Mem. tiorichi mcden<£{,
1793 ; Scharfcnberg, GtacK. dts Hercog^., Modena, 1S59 ; Oreste Bacgi, Modena
OatTiUa, 1860; Busldi, Storia di Modena; ValdTighi, Dii. Slorieo, is., delU
eo-alrade di Modena, 187^80 ; Crcsr<llaDi, Ouida di Modena, 1S79 ; Galvani, Men.
-A/T. intomo la riii di Franvjco IV., 4 vols.
MODICA, a city of Italy, in tne province of Syracuse
in Sicily, 8 miles from the south coast, on the line of rail-
way decreed in 1879 between Syracuse and Licata. It
has increased its communal population from 30,547 in 1861
to 41,231 in 1881, and is a well-built and flourishing place.
Of note among the public buildings are the old castle on
the rock, the mcdixeval convent of the Franciscans, and the
churches of S. Maria del Carmine (11. 50) and S. Maria di
Betlem — this last containing ruin<! of the ancient temjile
destroyed by the earthquake of 1693. Modica is the point
from which the remarkable prehistoric tomb and dwelling-
c^es of Val d'Ispica are usually visited. An early de-
pendency of Syracuse, Hotyca or ilutycu v-.is in Cicero's
days a fairly important municipium. Ir. modem times it
was held as a couutship by the dukes of Alba. Placido
Caraffa has written a prolix histor)' of the city, which may
be found in Grsevius, Thes. Ant. et Hist. Ital., vol xii
MOE, JoEGEX ExGEBEETSEN (1813-1882), Norwegian
poet and comparative mythologiit, was born at Hole in
Sigdal, Ringerike, Norway, on 22d April 1813, and entered
the university of Christiania as a theological student at the
age of seventeen. After leaving the university La 1839 he
acted as tutor in various schools and families, and in 1845
was appointed professor of theology in the 5Iilitary School
of Norway, which post he held until 1853, when he became
resident chaplain in his native parish of Sigdal. In 1863 he
received the living of Bragemsss, Drammen ; in 1870 that
of Vest Aker, near Christiania; and in 1875 the bishopric
of Christiansand, where he died on 27th March 1882.
Moe's first pubhcarion was a volume of 2s^orse "songs, ballads,
and staves," which appeared in 1S4D ; it was followed in 1841 by
the Si'orsls FoJkc-evenlyr (Norwegiin Popular Tales), which he had
collected along with his schoolfellow Asbjomsen. The work excited
such interest as a contribution to the study of comparative mythology
that in 1847 he was sent by the Government through Thelemark
and Sietersdal to increase his collection of stories. The second
(enlarged) edition, with a preface by Moe. appeared in 1852. In
1851 his I BTom'.cn 07 » Tjemet (In the Well and in the Tarn), a
delightful collection of prose stories for children, appeared, and it
was followed in 1S59 by a, volume of poems entitled Er., lulcn JuJcgave
(A Little Christmas Present). In 1877 he prepared a collected
edition of his works in two volumes, the stories he had published
along with Asbjomsen being excluded. Many of the Folke^evcntyr
(Popular Talcs from the It'</rsc) were translated by Sir George
Dasent in 1S59.
MCESLA (in Greek Mysia, or, to distinguish it from the
country of the same name in Asia, Mysia in Europe), in
ancient geography the territory immediately to the south ot
the Danube corresponding in the main to Servia and Bul-
garia. It became a Roman province between 27 B.C. and
6 A.D., probably about 16 B.c.^ In the time of Tiberius
and Caius the province was under the same governor with
Macedonia and Achaia. It was divided by Domitian into
two provinces, Mcesia Superior (Servia) and Moesia Inferior
(Bulgaria) ; and the same emperor completed the great
military road along the line of the Danube, increased the
strength of the Roman forces in the country, and, by the
conquest of Dacia, saved it from the inroads by which it
had been harassed from the time of Tiberius. The Goths
invaded Jlossia in 250 A.D., and at last, in 395, a number
of them, afterwards known as Moesogoths, obtained per-
mission to settle in the province. The Slavonians and
Bulgarians appear in the 7th century.
The boundary between Upper and Lower Mcesia was not marked,
as Ptolemy (iii 9, 10) states, by the river Cebrus or Ciabrus
(Cibritzacr Zibru), but, as may be inferred from an inscription (6125,
C. iTiAzr. Lat.j vol. iii. 2, additamenla), lay between Almus (Lorn)
and Ratiaria (Artcher). Upper Mcesia, or, as it was often called,
Mcesia Prima, contained — Singidnnum (Belgrade), headquarters
of Lcgio IV. Flavia, and in the 3d century a colonia ; Viniinacium
(Kostolatz), headquarters of Leg. VII. Claud., and designated some-
times municipium .ffilium, but more usually colonia (a rank bestowed
on it by Gordianus) ; Bononia (Widin) ; Ratiaria, which, on the loss
of Dacia, became the headquarters of Leg. XIII. gemina, and
remained a large town till it was destroyed by Attila ; Remesiana
(Mustapha Pasha Palanka), which has furnished inscriptions belong-
ing to the unidentified Ulpiana ; and Naissus (Nissa or Nish), tho
birthplace cf Constantine the Great. Lower Mcesia (Mcesia Sccunda)
contained— Ocscus (Colonia Ulpia, mod. Gigcn), headquarters, after
loss of Dacia, of Leg. V. Maced. ; Nova (Sistova), at a late date a
camp of Leg. I. ItaL, and afterwards chief seat of Thecdoric king
of the Goths ; Nicopolis ad Istrum (Nikup), really on the latrus or
Yantra, a memorial of Trajan's victory over the Dacians ; Pristra
(Rustchuk), Asamus (NicopoU on the Osma), Darostorum (Silistria),
Odcssns (Varna), Tomi (Kustendje), Troesmis (Iglit^a).
See Boe-JCT, flciMiifjcM Slarfitn, JSTl; Pfllmcr, Gesth. der B5n. Kaiaer-
leaitmtJi, ISSi, pp. 162161 ; Halm, in DJacltr. K. Ak. ier Wiu., rh. E. CX,
Viennm 1861. p. 228.
MOFFAT, a health resort of some note in Scotland, is
situated in Upper Annandale, Dumfriesshire, occupying Ml
' See A. W. Zmnpt, C'cmraci/af. Spiyrajrh., ii. 253 «jj.
M O F — M O G
543
agreeable position at the base of the Oatlow Hill, C3 miles
from Edinburgh, and 42 miles from Carlisle by railway.
The Spa, which is H mijea above the town (525 feet
above sea-level), is sulphureous with some saUne ingre-
dients, and is used in gout, rheumatism, and dyspepsia.
Population (1881) 2161 ; in the season about 4000.
MOFFAT, RoiiEKT', D.D. (1795-1883), African mission-
ary, was born at Ormiston, Haddingtonshire, Scotland, on
21st December 1795, of humble parentage. Moffat learned
the craft of gardening, but in 1814 offered liimscii to the
London Missionary Society, who, in 1816, sent him out to
South Africa. After spending a year in Namaqua Land,
with the powerful and dreaded chief Africaner, whom he
converted, Moffat returned to Cape Town in 1819, and
married Miss Mary Smith, a remarkable woman and most
helpful wife. In 1820 Moffat and his wife left the Cape
and proceeded to Griqua Town, and ultimately settled at
Kuruman, among the Bechuana tribes lying to the west of
the Vaal river. Here he worked as a missionary till 1870,
when he reluctantly returned finally to his native land. He
made frequent journeys into the neighbouring regions, as
.'or north as the Matabele country, to the south of tho
Zambesi. Tho results of these journeys he communicated
to the Eoyal Geographical Society (Jour. R. G. S., xxv.
xxviii., and Proc. ii.), and when in England in 1842 he
published his well-known Missionary Labours and Scenes
in South Africa. Single-handed he translated the whole
of the Bible into Bechuana. While solicitous to turn the
people to Christian belief and practice, Moffat was perhaps
the first to take a broad view of the missionary function,
and to realize tho importance of inducing the savage to
adopt tho arts of civilization. He himself was builder,
carpenter, smith, gardener, farmer, all in one, and by pre-
cept and example he succeeded in turning a horde of
bloodthirsty savages into a "people appreciating and
cultivating the arts and habits of civilized life, with a
written language of their own." Now wo find more or less
Christianized communities extending from Kuruman to
near the Zambesi. Moffat met with incredible discourage-
ment and dangers at first, which he overcame by his strong
faith, determination, and genial humour. It wa^ largely
due to him that the work of Livingstone, his son-in-law,
took the direction which it did. On his return to England,
Moffat received a testimonial of about £6000. He died
at Leigh, near Tunbridge Wells, 9th Aug. 1883.
See Scenes aiid Services in South Africa, the Story of Moffat's
?fis3ioivirif Labours, London, 1876 ; and publications of the London
Missionary and tho B. and F. Bible Societies.
MOGADOR, or Suerah (Berber TasuH), the most
Eouthem seaport town on the Atlantic coast of Morocco,
and the capital of the province of Haha, stands from 10
to 20 feet above high water on a projecting ridge of cal-
careous sandstone in 31° 30' N. lat. and 10° 44' W. long.
In certain states of wind and sea it is turned almost into
an island, and a sea-wall protects the road to Saffi. The
streets are regular and, for a Moorish town, broad and clean.
Witliin tho walls there are three distinct divisions : the
citadels old and new with the government buildings; to
the north-west the outer town with its spacious markets
in the centre ; and at the north-west comer the Mellah,
or Jews' quarter. In the citadels the houses are fairly
good, and considerable attention is paid to sanitary matters.
^Vate^ is brought from the Kseb, about IJ miles to tho
south, by an aqueduct. The prosperity of Mogador is due
to its commerce ; only a few gardens break the barren-
ness of the immediate vicinity. The harbour or roadstead,
though apparently protected by the island and quarantine
Ktation of Mogador, is extremely dangerous during west
and south-west winds. Trade is carried on mainly with
Marae'lles. London, Gibraltar, and the Canaries — the prin-
cipal exports being almonds, goat-skins, gums, Olive oil,
and ostrich feathers, and the principal imports cotton goods
(half of the total) and tea. The average v&lue -oi tha ex-
ports for the five years 1877-1881 was about £210,000, the
imports rather less. Attention has been frequently directed
to the value of Mogador as a health resort, especially for
consumptive patients. The climate is remarkably steady :
mean temperature of the hottest month 71 06, of coldest
month 58-69. The annual rainfall is only 10 or 12 inches,
and the rainy days of winter and spring about 28. The
sirocco is but rarely felt. The population is about 15,000
(7000 Jews, about 150 foreigners). Jews, Protestants,
and Roman Catholics have religious edifices in tho town.
A place called Moj^ador is marked in tho 1 Siil Povtiilan of the Lau-
rentian Library, and tho map iu Hondiiis's Atlas Minor shows the
island of ]\logador /. Do7nc(jador ; but the oripn of tlio present town
is much more recent. Mogador was founded by Sultan Jlohamniod,
and completed i]i 1770. The town received from tho Moors the
name of Suerah (little picture), while the Portuguese called it after
the shrine of Sidi Mogadul, which lies towai-ds tho south half-way
to tho village of Diabat, and forms a striking landmark for seamen.
In 1844 tho citailtl was bombarded by the French.
MOGHILEFF, a north-western government or pro-s-ince
of the Russian empire, situated on the upper Dnieiier,
between the provinces of Vitebsk and Smolensk on the
north and ea.4, Tchernigoft' and ]*[insk on the south and
west. In the north it is occupied by the watershed which
separates the basir* of tho Dwina and tho Dnieper, an
undulating tract from 650 to 900 feet above the sea-level,
and covered nearly everywhere with forests. This water-
shed slopes gently to the south, that is, to the valley of
the Dnieper, which enters the province from the north-
east and flows west and afterwards due south. The
southern part of tho province is flat and has tnuch in com-
mon with the Polyesie of the province of Minsk ; it is,
however, more habitable, the marshes being less extensive.
The province is covered by the Tertiary formation ; Devonian
sandstone appears in the north, and Carboniferous limestones in the
cast. The soil is mostly sand, clay (brick-clay and iiotter's-clay arc
not uncommon), and jKat-bogs, with a few patclies of "black-
earth." The climate is rude and wet, the average yearly tempera-
ture at the Gorki moteorological observatory being 40° *4 Fsitir,
(14°*2 in January, and 63°*8 in July) ; cold nights m summer are
often the cause of bad crops. The province has about 1,140,000
inhabitants (9-17,625 in 1870), mostly White -Russians (78 pel
?:ent.), bi^longing to the Greek Church ; Jews are numerous (16 per
C'-int.) ; Poles, belonging mostly to the nobility, mako only 3 per
cent, of the population. Agriculture is the chief occupation ;
nearly one half (46 per cent.) of the surface of the pronnce is under
crop ; but, except after unusually good harvests, corn is imported,
chiefly by the navigable channels of the Dnieper and SozIl There
are many distilleries on tho estates of landowners, and wine-spiril
is exported. The hemp culture is import-ant ; hemp and hemp-
seed oil are exported to Riga. Tho province has one large paper-
mill, a few iron and copper works, and minor manufactures.
Tho province of MogliilefT is divided into eleven districts, with
the chief towns : Jloghileff (40,500 inhabitants), Ohausy (4200),
Tcherikoir (3900), Gomel (13,030), Gorki, formerly the seat of an
agricultural institute (5050), Klimovichi (4000), Jlstislavl (6700),
Orsha (5350), Rogachetf (7750), Staryi Bykholf (5200), and Syenno
(2550). Of about 80 other municipal towns, we name Shkloff
(13,000 inhabitants), Dubrovka (7000), Kricheff (4000).
■This province was inhabited in the 10th century by the Krivichi
and RadimichL In the 14th century it became part of Lithuania
and afterwards of Poland. Russia annexed it in 1772.
MoGHiLEFP ON THE DNIEPER, a town of Russia, capital
of the province of same name. It is situated on both
banks of the Dnieper, 40 miles south of the Orsha station
of the railway between Moscow and Warsaw. A railway
along the Dnieper will soon bring Moghileff iuto railway
communication with these capitals.
MoghiUir is mentioned for the first time in the 14th century
as a dependency of the Vitebsk, or of the Mstislavl principality.
At the beginning of the 15th century it became the personal
property of the Polisli kings. But it was continually plundered
— either by Russians, who attacked it six times during tho
16th century, or by Cossacks, wlio plundered it three times. Id
tho 1 7th century its inhabitants who belonged to the Greek Church
-"flercd muoJ.'' from th» persecutions of tho Union. lof lfi£4
544
M 0 G-^M O H
it surrendered to 'i;iissia," but" in 1661 the Russian garrison vas
massacred by the inhabitants. In the 18th century it was taken
several times by Russians and by Swedes, and in 170S Fetor I.
ordered it to be destroyed by fire. It was annexed to Russia in
1772. Of 40,500 inhabitants two-thirds arc Jews and the remainder
AVhite-Russians, with a few Poles (2500). Its m.inufactures are
without importance ; but one branch of trade, namely, tlie prepa-
ration of skins, has maintained itself for many centuries. The
commerce is mostly in the hands of Jews : com, salt, sugar, and
fish are broURht from the south, whilst skins and manufactured
ware imported from Germany (partly by smugglersl are sent to the
southern provinces.
MOGHILEFFoNTHEDNTESTER(J/oA;;oij),adtstricttown
of Russia, situated in the province of Podolia, on the left
bank of the Dniester, 87 miles east-south-east of Kamenets-
Podolsk, and 43 miles from the Zhmerinka railway junc-
tion. It has 18,200 inhabitants, nearly one-half of whom
are Jews ; the remainder are Little Russians, Poles (1500),
and a few Armenians. The Little-Russian inhabitants of
Moghileff carry on agriculture, gardening, wine, and mul-
berry culture. The Jews and Armenians are engaged in
a brisk trade with Odessa, to which they send corn, wine,
spirits, and timber, floated down from Galicia, as well as
wth the interior, to which they send manufactured wares
imported from Austria.
Jloghileff, named in honour of the Moldavian hospodar Mohila,
was founded by Count Potocki about the end of the 16th century.
Owing to its situation on the highway from Moldavia to the Ukraine,
at the passage across the Dnieper, it developed rapidly. For more
than 150 years it was disputed by the Cossacks, the Poles, and the
Turks. It remained in-the hands of the Poles, and was annexed
to Russia in 1795. The Crown purchased it from Count Potocki
in 1806.
SIOGLLAS, Peteus (c. 1600-1647), metropolitan of
•Kieff from 1632, belongfed to a noble Wallachian family,
and was bom about the year 1600. He studied for some
time at the university of Paris, and first became a monk
in 1625. He was the author of a Catechism (KieflF, 1645)
and other minor works, but is principally celebrated for
tlie Orthodox Cim/ession;-^Ta.vm up at his instance by the
ijibbot Kosslowski of EaeflT, approved at a provincial synod
^n 1640, and accepted by the patriarchs of Coastantinople,
'Jerusalem, Alexandria and Antioch in 1642-3, and by
the fsynod of Jerusalem in 1672. See Greek Chdtich,
vol. xi. p. 158.
Tlicre are nnmerons editions of the Confession in Russian ; it has
been edited in Greek and Latin by Panagiotcs (Amsterdam, 1662),
hy Hofmann (Leipsic, 1695), and by Kimmel (Jena, 1843). and
tiierc is a Gcnnan translation by Frisch (Frankfort, 1727).
JIOGUL, or Mughal, Ji., the Arabic and Persian
form of the word ^longol, usually applied to the Mongol
empirerfin India. See India, vol. xii. p. 793 sqq.
MOH ACS, a market town in the Trans-Danubian county
of Baranya, Hungary, stands on the right bank of the west
arm of the Danube, 25 miles east-south-east of P6c3 (Fiinf-
kirchen), with which it is connected by railway, 45° 58' N.
lat., 18° 37' E. long. At MohAcs there are several churches
and schools belonging both to the Roman Catholics and
the Calvinists, also the summer palace of the bishop ot
P&3, a monastery, an old castle, and a -station for steamers
plying on the Danube, by which means a considerable
commerce in wine and the agricultural produce of the
neiglibourhood is carried on with Budapest and Vienna.
Not far from MohAcs are coal mines, and the town is an
important coal depot of the Danubian Steam Navigation
Company. Tho popidation in 1880 was 12,047 (Magyars,
Serbs, and Germans).
Two great battles fought in tho vicinity of tho town mark tho
commem^ernent and close of tho Turkish dominion in Hungary.
In tho first, 29th August 1526, tho Hungarian army under Louis
II. was annihilated by the Ottoman forces led by Soliman tho
Ma^ificent (see voL xii. p. 369). In the second, 12th Au^ist
1687, tho Austiians under Charles of Lorraine gained a great and
decisive victoiy over the Turks, whono power was afterwards still
further broken by Prince Kugcno of Savoy.
MOHAIR is the woolly hair of a variety of the common
or domestic goat inhabiting the regions of Asiatic Turkey,-
of which Angora is the centre, .whence the animal is known
as the Angora Goat (see . Goat, vol. i. p. 708). Goat's
hair has been knovra and used as a textile material in the
East from the most remote periods ; but neither the Angora
goat nor its wool was known in Western Europe till, in
1655, the animal was described by the naturalist Tourne-
fort. That textures of mohair were in use in England
early in the 18th century is obvious from Pope's allusion ;—
* ' And, when she sees her friend in deep despair.
Observes how much a chintz exceeds mohair."
Owing, however, to the jealous restrictions of the Turkish
power, it was not till 1820 that mohair became a regular
article of import into the United Kingdom. In that year
a few bales came into the market ; but so little was the
material appreciated that it only realized lOd. per ft. In
1870 average mohair fleece was selling at five times that
price. , From the small beginning of 1820 the imports
gradually waxed, and the trade received a very consider-
able impetus through the introduction in 1836, by Titus
Salt, of the analogous fibre alpaca. The increasing demand
for and value of mohair early stimulated endeavours to
acclimatize the Angora goat in other regions ; but all
European attempts have failed, owing to humid and un-
genial climates. In 1849 a flock was taken by Dr J. P.
Davis to the United States of America, and since that
time many fresh drafts have been obtained and distributed
to Virginia and various Southern States, and to California
and Oregon in the west. In these high and dry regions
the goats thrive ; and the flocks in the Western States
now number many thousands. The Angora goat has also
been introduced into the Cape of Good Hope with much
success. The first importation of mohair from the Cape,
made in 1862, amounted to 1036 ft ; and now about one-
tenth of the total British supply is received from that
source. Mohair has also been received in England from
goats reared successfully in Fiji, where they were first in-
troduced in 1874, and there are also thriving flocks in
Australia.
The trade in mohair between Asia Mijior and western Europe U
controlled in Constantinople. There upwards of twenty varieties
of fleeces are distinguished according to the localities of their pro-
duction, the richest and most lustrous qualities being produced In
hilly and forest regions, while the fleeces from the open plains arc
comparatively kempy, coarse, and cottony. From the Lake Van
district on the eastern borders of Asiatic Turkey a distinct and
inferior variety of wool is obtained. It is known in commerce ag
Van mohair, and consists, to theextent of about 70 jwr cent., of white
wool slightly streaked with black, with 30 per cent, of coloured red
and black wool. At Konieh in the south, also, an inferior mohair
known as Polotons is produced, 80 per cent, of which ia black and
red, and the remainder white. The average weight of an Angora
goat fleece is from 5 to 6 lb. The finest quality of wool is obtained
from the first clip, which is made in the second year of the animal.
She-goats yield the best wool, after which coino wethers, while
the rams give the coarsest fleeces. Angora mohair is a brilliant
white lustrous fibre, elastic and wiry in character, and devoid of
felting properties. It attains the length of four or five inches, but
the long fibre is mixed ^vith an undergrowth of shorter wool, which
in tho spinning process is combetl out as " noils " for separa*,o use.
It is a material of enormous durability, and, owin^; to its remarkable
elasticity, it is especially fitted for working into long piled fabrics,
such as plush and imitation furs, or for use in braids and bindings,
and in boot and other laces. It is largely used for making Utrecht
velvet or furniture plush for the upholstering of railway carriages,
iic, a trade centred at Amiens. In the making of imitation seal-
skins, and imitation beaver, otter, chinchilla, and other fui-s, and
for carriage rugs generally, mohair is extensively employed. Many
dress fabrics of mixed mohair and alpaca, cotton, or silk are also
manufactured ; but with changes in fashion such materials are con-
stantly changing in style, composition, and name. Mohair is also
used for making certiin qualities of lace, and an imitation of ostrich
fcatliers for use as trimming has been made from the fibre. The
imports of mohair into the United Kingdom during 1882 amounted
to 16,859,771 n>, valued at £1,433,531, a quantity Idrgoly in excess
of the imports of any pro\ioiis year.
VOL.X\'l
ITISM
PLATEYm.
545
MOHAMMEDANISM
■Undee this head is given the history of Mohammed and
his successors to the fall of the Eastern Caliphate, ■nith a
sketch of the institutions and civilization of the Moslem
empire and an account of the Koran. The later history
must be sought unaer the names of individual countries and
dynasties. What falls to be said of the social and religious
aspects of Lslam in modern times will be given under the
two great divisions of Susxites and Sni'iTES.
PART L— MOHAMMED AND THE FIEST FOUR CALIPHS.
.rabia.Tl
16 biril
MOHAMMED! or MAHOMET, the founder of Islam,
first appears in the full light of history with his
Flight to Medina (The Hijra), a.d.' 622 ; and this date,
not that of his birth, bus been fittingly chosen as the
epoch of the Moslem Era. The best-attested- tradition-
places his first appearance as a prophet in Mecca some
twelve years earlier {circa 610). He was then forty years
old : the forty must be taken as a round number, but as
such is doubtless trustworthy. Thus the birth of Moham-
med falls about 570 a.d. : it is said to have fallen in the
year when AbrahA, the Abyssinian viceroy of Yemen, made
the expedition against Mecca, mentioned in the Koran,
when the Arabs first saw the elephant and first suffered
from smallpox.'
; At the time of Mohammed's birth and youth nothing
' seemed less likely than that the Arabs should presently
make their triimiphal entrance into the history of the
world as victors over the Greeks and Persians. Nowhere
in the Peninsula was there an independent state of any
considerable power and importance. At the beginning of
the 6th century indeed the princes of Kinda had attempted
to form a national kingdom, uniting in particular the
tribes of central Arabia ; but this kingdom was nothing
more than an epic prelude to the true history of the Arabs,
which begins with Islam. After the fall of the Kindite
dynasty, the old anarchy reigned again among the nomada
of the Nejd and the HijAz ; in all other quarters Greek or
Persian influence predominated, extending from the frontier
deep into the interior by the aid of two vassal states — the
kingdom of the Ghassanids in the Haurin under Greek
suzerainty, and that of the Lakhmids iu Hira and Anbdr
under the Persian empire. The antagonism between By-
zantium and Ctesiphon was reflected in the feuds of these
Arab lordships ; but indeed the rivalry of Greek and Persian
exercised its influence even on the distant South of the
Peninsula. Urged on by the Greeks, the Abyssinians had
overthrown the Christian-hating realm of the Himyarites,
the sunken remnant of the ancient might of the Sabaeans
(a.d. 526), the Persians had helped a native prince again
to expel the Christians (circa 570), and since then the
Persians had retained a footing in the land. Toward the
close of the 6th century, their direct and indirect influence
^ The name Mohammad means in Arabic "the praised," and it has
been supposed that this epithet was conferred on the Prophet after his
mission to mark him out as the promised Paraclete. Tliis, however,
is incorrect (Noldeka, Gesch. d. Qoram [Gdtt. 1S60], p. 6, note 2;
Sprenger, Leben und Lekre des AT, i. 155 sq.) The name is found,
although it was not common, among the lieatfaen Arabs. Renau has
fihown it to occur on a Greek inscription of the early part of the 2d
centurj- of the Christian era (Boeckh, C. I. C, 4300), and Mohammed
ibn Maslama of Medina, a contemporary of the Prophet, bore it as his
original name, as appears from the fact that his brother was called
Mahmud, it being a favoarite practice to give to brothers variations of
the same name, as jinas and Minis, Sahl and Sohail, Monabbih and
Wobaih (Sprenger, i. 158, note 2). That Mohammed calls himself
Ahmad, in sur. IxL 6, in order to adapt bis name to a supposed pro-
phecy, proves nothing ; on the other hand, the men of Mecca, on occa-
sion of a tieaty with the Moslems, demanded that the Prophet shoild
not call himself messenger of God, but Mohammed ibn 'Abdallih,
using his old familiar name; see J. Wellhauseu, VaJndi'a Kifub al-
Maghaziin verk&rzter deiUsdier ^yiedergahe {^i\. 18S2),.p. 257.
^ Niildeke, ut supra, p. 54 sq.
' Noldeko, Getch. d. Perser und Araicr ntr Zeil der Siuanidcn
«iu . . . Tabari ibersetst (Leyden, 1879), pp. 205, 218.
in Arabia greatly surpassed that of the Greeks ; and since
the Kindites had fallen before the kings of Hiia, it extended
right through the Nejd into Yemen. ^
In the Hijaz and western Nejd, the district from which
Islam and the Arab empire took their beginning, Greeks
and Persians, Ghassanids and Lakhmids, had not much
influence ; the nomad tribes, and the lew urban common-
wealths that existed there, lived free from foreifjn interfer-
ence, after the mannfr of their fathers. Jlohammed's city
was Mecca, where the Banii Kindna had formed a settle- Mc
ment roimd the Ka'ba, the sanctuary of a number of con-
federate tribes (AhAblsh) belonifing to that district. The
feast annually observed in the days before the full moon of
the month Dhii '1-Hijja at Mecca and at 'Arafa and Kozah in
the vicinity, presented strong attractions for all inhabitants
of the Hijdz, and grew into a great fair, at which the
Meccans sold to the Bedouins the goods they imported
from Syria. Feast and fair gave the city the prosperity
which it shared with other cities which, like Mecca, had
the advantage of lying near the meeting-place of the two
great natural roads to Yemen — that from the north-west
along the Red Sea coast, and that from the north-east fol-
lowing the hue of the mountains that traverse the Nejd.'
By their trading journeys the Koraish" had acquired a
knowledge of the world, especially of the G.»seco-Syrian
world : the relative superiority of their culture raised them
not only above the Bedouins, but above the agricultural
population of such a city as Medina ; the art of reading
and writing was pretty widely diffused among them. The
Koraish within the city were the Banii KaTj ibn Loay,
those in the surrounding country Banii 'Amir ibn Loay ;
the townsmen proper were again subdivided into Jlotayya-
biin and AhUf — the latter were the new citizens, who wera
distinguished from the old settlers by the same name in
other Arabian towns, as in Taif and Hira. The community
was a mere confederation of neighbouring septs, each
occupying its own quarter ; there was no magistracy, the
town as such had no authority. All political action centred
in the several septs and their heads ; if they held together
against outsiders, this was due to interest and a sense of
honour, a voluntary union strengthened by the presence
of public opinion. In the time of Mohammed, the most
numerous and wealthy sept was that of the Banii Makhziim ;
but that of the Banii 'Abdsha^is was the most distinguished.
The Banii Omayya were the most powerfid house of "Abd-
shams ; their head, Abii Sofyin ibn Harb, exercised a de-
cisive influence in the concerns of the whole community.
Mohammed himself was of the Banii Hiishim; it is afiirmed
that these had formerly enjoyed and claimed of right the
position actually enjoyed by the Banii Omayya, but thia
assertion seems to have had its origin in the claims to
the Caliphate which the Hashimites (the house of 'Ali and
the 'Abbdsids) subsequently set up against the Omajyads.^
* On the state of Arabia before Islam see Caussiu de Perceval, Essai
Siir Vhistoirt des Arabes, vol, ii, ; Mtiir, Li/e of Mah., vol i.
* Marr al-Zahran, near Mecca, is accordingly said to have been the
point at which the great emigration of tribes from Yemen p.arted into
two streams, moving north-west and north-east respectively.
* The Koraish were the branch of Kinana settled in and abont
Mecca. They are called also Ghdlib and Fihr, but the last name i«
particularly applied to tliose of the Koi-aish who did not live withia
the town. ' Sprenger, vol. iil p. cix. *j.
XVI. — 6q
546
MOHAMMEDANISM
[hohakmed.
Tooth of Mohammed's father, 'Abdalldh b. 'Abdalmottalib, did
the Pro- not live to see the son's birth, and his mother Amina
pl'ft- died wliile he was still a child. Mohammed was then
cared for first by his grandfather, "Abdalmottalib, and
after liis death by his oldest paternal ilncle, Abii Tdlib
b. "Abdalmottalib. He. was kindly treated, but shared
the hardships of a numerous and very poor family ; he
herded sheep and gathered wild berries in the desert.
This is all that we know of his youth (sur. xciii. 6), all
else is legend, containing at roost an occasional fragment
of truth.i
It was, we are told, in his twenty-fifth year that
Mohammed, on the recommendation of his uncle, entered
the house and business of a wealthy widow named Khadija.
For her he made commercial journeys, thus learning to
know part of Palestine and Syria, and perhaps receiving
impressions which fructified in his soul.- By and by he
married the widow, who was much his senior ; he was a
shrewd man, with prepossessing countenance, fair of skin,
and black-haired. The marriage was happy, and blessed
with several children. The two sons, however, died young;
from the elder the father received the surname Abil '1-
KAsim. The most famous of the daughters was Fitima,
who married her father's cousin, 'Ali b. Abl T^lib.
Arabian During his married life with Khadija, Mohammed came in
K'.igioD. contact with a religious movement which had laid Hold on
some thoughtful minds in Medina, Mecca, and T^if- In
Mecca, as elsewhere, Arabian heathenism was a traditional
form of worship, chiefly concentrated in great feasts at the
holy places ; it was clung to because it had come down
from the fathers. The gods were many ; their importance
was not due to the attributes ascribed to them, but to
their connection with special circles in which they were
worshipped. They were the patrons of septs ' and tribes,
and symbolized, so to speak, the holy unity which united
the present and past members of these. Above them all
stood Allah, the highest and universal God.* By him the
holiest oaths were svvorn ; in his name {Bismika Alldhummd)
treaties and covenants were sealed ; the lower gods were
not fit to be invoked in such cases, as they belonged to one
party instead of standing over both. The enemy was re-
minded of Allah to deter him from inhuman outrage ;
enemy of AUAh ("aduw AUAh, ^coo-TuyTJs) was the name of
opprobrium for a villain. But, since Allih ruled over all
' * The tradition relates that as an infant Mohammed was entrusted
/to a Bedouin foster-mother, Halima, who brought him up among her
ipeople, the Banu Sa'd b. Laith. Sprenger (I 162 sq.) will have it that
■this precise statement is also a fiction ; but he is probably wrong. It
'can hardly be disputed that Bedouin women were accustomed to suckle
'the children of townsfolk for wages, and Mohammed's "milk-kinship "
with the Banu Sa'd b. Laith is confirmed by what happened at and
after the battle of Honain. A nephew of Mohammed was .also
brought up among the Sa'd. Comp. Vakidiy ul supra, pp. '364, 377 sq,,
431, note 1.
' = He saw the mute witnesses of divine judgment, the rock-dwellings
of Hijr and the Dead Sea ; perhaps, too, he was impressed by the
figure of some venerable monk (Bahira legends). Comp. Ibn Hishdm,
p. 115 sq.; Sprenger, i. p. 178 sqq,
|. » Vakidi, p. 350 : IdoU were found in every house, and homage
Wai paid to them when men wont out or in to gain their blessing. Abii
Eajrat made and sold them ; there was a lively trade in idols with the
Bedouins.
y * The particular gods are said to have been regarded as children of
AUih (D^n^K '33)- From sur. liiL 21, xxxvii. 149, it appears that
the Mcccans called their goddesses daughters of Alldh ; perhaps
it was their disputes with Mohammed that forced them to this view.
At first, certainly, al-L4t and nl-'07.z.4 were names of the wife of the
supreme god ; sexual dualism dominated in the oldest Arab idea of
tho godhead. It was Mohammed who first reduced the gods to
Jlnns — i.e. to subordinate demons and kobolds — as be did not deny
).heir eiktence, but only stripped off their divinity. To say that the
oldest Arabs worshipped Jinns is .is unre.isonable is to say that they
Worshipped the devil ; for Islam degiaded the gods to Shnitins as well
03 to Jinns. Superstition certainly played its port among the Arabs,
l>nt.6uperBtitiOQ is not rvUgiqn,
and imposed duties on all; it was not thought that one
could enter into special relations with Jiim. In worfldp
he had the last place, those gods being preferred who
represented the interests of a specific circle, and fulfilled
the private desires of their worshippers.' Neither the fear
of AJldh, however, nor reverence for the gods had much
Influence. The chief practical consequence of the great
feasts was the observance of a truce in the holy months,
and this in course of time had become mainly an affair of
pure practical convenience. In general, the disposition of
the heathen Arabs, if it is at all truly reflected in their
poetry, was profane in an imusual degree. Wine, the
chase, gaming, and love on the one side ; vengeance, feuds,
robbery, and glory on the other, occupy all the thoughts of
the old poets. Their motives to noble deeds are honour
and family feeling ; they hardly name the gods, much
less feel any need of them. The man sets all his trust on
himself : he rides alone through the desert, his sv^-ord helps
him in danger, no God stands by him, he commends his
soul to no saint. His reckless egoism may expand to noble
self-sacrific for the family and the tribe ; but in this
heroism religious impulses have no part, there is nothing
mystical in these hard, clear, and yet so passionate natures.
The only vein of what can in any sense be called religious
feeling appears when the volcano has burned itself out and
the storm of life is over ; then, it may be, a wail is heard
over the vanity of all the restless activity that is now
spent.^ It is very possible that religion meant more to tho
sedentary Arabs than to the nomads, to whom almost all
the ancient poetry belongs ; but the diilerence cannot have
been great. The ancient inhabitants of Jlecca practised
piety essentially as a trade, just as they do now ; their
trade depended on the feast, and its fair on the inviolability
of the Haram and on tho truce of the holy months.'
The religion of the Arabs before Moliammed was de- 1
crepit and effete.' Many anecdotes and verses prove that '
indifl'erence and scoffing neglect of the gods was nothing-
uncommon. The need for a substitute for the lost religitin
was not very widely felt. But there were individuals who
were not content with a negation, and sought a better re-
ligion. Such were Omayya b. Abl '1-Salt in Tiif, Zaid b.
"Amr in Mecca, Abii Kais b. Abi Anas, and Abii 'Amir in
Medina.' They were called Hanlfs, probably meaning
» Vakidi, pp. 3CS, note 1, 370, note 1 ; Sprenger, iii. 457 sq., 512.
'Whether the feast at Mecca was celebrated in honour of AllAh before
Mohammed, is very doubtful. It would seem that Hobal w-as wor-
shipped in the Ka'ba {Ibn Hisham, p. 97 sq.), and Kozah in Mozdalifa
{Vakidi, p. 428); it is possible, however, that Allah stood to Hobal
among the Arabs as El to Jnhw^ among the Hebrews. Ritual sacri-
fices were generally presented to a god who had a proper name ; but
the trace of a religious rite which still survived in the ordinary killing
of beasts for food, possibly rnn:.;stcd even before Mohammed in the
invocation of the name of All.-ih (Spi-enger, ii. 478, note 1; but comp,
Vakidi, p. 160, note 1, p. 168).
* '*We hasten towards an unknown goal, and forget it in eating and
drinking. We are sparrows and flies and worms, but more daring
than famishing wolves. . . . My roots reach down to the depths of tho
earth ; but this Death spoils me of my youth, and of my sotj he spoils
me and of my body, and right soon lie lays me in the dust. I have
urged my camel through every desert, wide-stretching and shimmering
wlh mir,Tgo ; and I have ridden in the devouring host, reaching after
the honours of greedy perils, and I joined in the fray under every sky
till I longed for the home-coming instead of booty. But can 1,
after Harith's death, and after the death of Hojr, the noblo host — can
I hop'e for a softer lot from the change of time, which does not forget
the liard mountains? I know that I must soon be transfixed by hij
talon and tooth as befell my father and my grandsii-e, not to forget him
that was slain at Koldh." — Amraalkais, cd. Slane, No. 10, p. 33;
cd. Ahlwardt, No. 5. - ~ - ~ -j
^ Sec, on Arabian heathenism, Tococke, Specimen hist Arabumj
Krehl, Religion dcr vorislamisdien Arabcr (Leip. 1863); Sprenger,'
i. 241 sq. • Vakidi, p. 293, noU 1. ^ ^ ^ ■>
• See, for Omayya, Kitib al-Aglidnl (Bilik ed.>, iii. _186 tq. / foi
Zaid, Ibn Hishim, p. 143 sq. ; for Abii Kais, id. 348 sq., 39 sq. ; «nij
for Ab(i 'Amir, Vakidi, pp. 103, 161, 190, 410.
)COHAXU£D.]
M.O HAMMED AN ISM
547
"penitents", men vrio BtriveTolree themselves from sin.^
They did not constitute a regular sect, and had in fact no
fixed and organized views. They had, no doubt, inter-
course with one another, but were not a close society; they
thought more of their own souls than of propaganda ; only
in Medina they seem to have been more niunerous. They
rejected polytheism and acknowledged Allih, but not so
much on intellectual grounds as on grounds of conscience.
Faith in the one God was with them identical with pious
resignation (Isldm) to his will ; their monotheism was most
closely aUied to the sense of responsibility and of a coming
judgment ; it stood opposed to the worldly ideas of the
idolaters, and was an impulse to upright and sin-avoiding
walk. They were not theorists, but ascetics. It was the
[Primitive ideas of Law and Gospel (" the religion of Abra-
3iam'") that Uved again in them. They felt on the whole
less attracted towards the developed forms of the religion of
fiBvelation; they rather sought after some new form ; few of
them attached themselves to existing religious communities.
' Mohammed, it would appear, came into connexion with
these Hanifs through a cousin of his wife, Waraka b.
Naufal, who was one of them. Their doctrines found a
frjiitful soil in his heart ; he was seized with a profound
isense .of dependence on the omnipresent and omnipotent
Lord, and of responsibility towards him. Following the
example of old Zaid b. 'Amr, he no'se frequently withdrew
lor "considerable periods to the solitude of the bare and
desolate Mount Hiri, and meditated there with prayer
and ascetic exercises. For years, perhaps, hfO went on in
thpse purely individual exercises, without anything to dis-
tinguish hm essentially from the others who helcL similar
views. But in him the Hanifite ideas lodged themselves
in a natural temperament which had a sickly tendency to
excitement and vision, and so produced a fermentation that
ended in an explosion.^ ■ Thus he became a prophet ; he
felt himself constrained to leave the silent circle of ascetics
and make a propaganda for the truth. In this resolve he
was unquestionably influenced by what he knew of the
example of the BibUcal prophets, perhaps also by the cir-
cumstance that a longing after a new founder of religion
was diffused among the Hanifs, and found support in some
dim acquaintance with the Messianic hopes of the Jews,
JeaiA That Mohammed did not independently produce his own
«J>d ideas is indisputable ; nor is it to be doubted that he de-
^l"f '"^ rived them from the Hanifs. But what was the ultimate
source of these first motions towards Islam ! In general
they are ascribed to a Jewish source. Jews were very
numerous in Hij4z and Yemen, and had perfectly free
intercourse with the Arabs, to whom they undoubtedly
imparted a quantity of Biblical and religious material
Mohammed in particular was mdebted to the Jews for
almost all the stories and a great part of the laws of the
Koran (laws of marriage, purity, etc.), and the theological
language of Islam is full of Jewish words. But the ori-
ginal and productive forces of Islam did not spring from
Judaism, least of all the ideas of the Judgment and of the
inexorable demands set before the creature by his Creator,
^ Sprcnger (p. 38 sq.) connects Hanif with 13PI, and expounds it
per antiphrasin as htciis a mm lucendo, on the ingenious fashion of
A. Geiger. As tahannuth = iahannuf is the technical name of such
solitary ascetic practices as llohammed himself engaged in before his
call, Hanif may be taken to mean a muiaJtannifby profession. The
connexion between Tuini/ and tahannvfi^ certain, and it seems equally
certain that taJmnnuf as an equivalent of tahannuth comes not from
fuinif but from hirUh (for hinf), and means not to play the Hanif but to
concern oneself with one's sin, to purge oneself of it.
^ It is disputed v/hether Mohammed was epileptic, cataleptic, hys-
teric, or what not ; Sprenger seems to think that the answer to this
medical question is tlie key to the whole problem of Islam. It is
certain that he had a tendency to see visions, and suffered from fits
which threw him for a time into a swoon, without loss of inner con-
•fiousuess.
which are so dominant in the older siiras, A distinction
must be drawn between the primitive impulses and the
material added later ; Mohammed did not get his leaVen
from the Jews, they only supplied him afterwards with
meal Neither in truth can Christianity be viewed as the
proper source of Islam — Christianity, that is, in any of
■its great historical developments. The Arabs knew Greek,
Syrian, and Ab3rssinian-Himyaritic churches ; manifold in-
fluences from these doubtless reache.l Islam, but in none
of them did the idea of Judgment still stand as the central
point of religion ; the living sense of divine reality ruling
over the life was half extinguished by the developments of
theology. But in the Syro- Babylonian desert, off the line
of the church's main advance, primitive forms of Chris-
tianity, perhaps also of Essenism, still survived, which the
course of chiirch history had left untouched. To these belong
on the one hand the Sabians (" Baptists," from J)3i'), on the
other the numerous anchorets of these regions. The con-
nection of Islam with the Sabians appears from the fact
that in Mecca and T^if its adherents were simply known
as Sabians.' From them, however, were derived, it would
seem, for the most part only externals, though the import-
ance of these must on no account be undervalued. The
deepest influence exercised on the Hanifs, and through
them on the Prophet, appears to have come from the an-
chorite ascetics. How popular they were with the Arabs,
appears from the Bedouin poetry ; what power they exer-
cised over the minds even of the heathen, is proved by
various episodes in the history of GhassAn and Hlra ; how
well the Arabs knew this difference between them and the
shaven clergy, is seen in the instructions of Abilbekr to the
commanders in the Syrian campaigns. It was not their
doctrine that proved impressive, but the genuine earnest-
ness of their consecrated Ufe, spent in preparation for the
Ufe to come, for the day of judgment, and forming the sharp-
est contrast to the profanity of heathenism. Ascesis and
meditation were the chief points with the Hanifs also, and
they are sometimes called by the same name with tha
Christian monks.* It can hardly be wrong to conclude'^
that these nameless witnesses of the Gospel, unmentionedi
in church history, scattered the seed from which sprang
the germ of Islam.
The tradition gives a telling story of the way in wmcn Mohai
Mohammed at length came to proclaim openly what had raed'e
long been Uving and working within him ; in other words, • .'
how he became a prophet. Once, in the month of Rama-
dan, while he repeated his pious exercises and meditations
on Mount Hiri, the angel Gabriel came to Jiim by night
as he slept, held a silken scroll before him and compelled
him, though he could notread, to recite what stood written
on it.* This was the first descent of a passage of the
heavenly book, the source of revelation from which Moses
and Jesus and all prophets had drawu; and so Mohammed
was called to be a prophet. The worfls with which Gabriel
had summoned him to read, remained graven on his heart.
They were the beginning of sur. xcvi. —
' Ibn Hishim (p. 835) relates that the Bauii Jadhima announced
their conversion to Islam to Khilid in the words, " We are become
Sabians." Kenan, .Siudes d'Aisfoire «I. (1863), p. 257, misunderstands
this utterance.
* Abii 'Amir is as often called Rihlb as Han(f. All the accounts
indicate that the Hanifs stood nearer to Christianity than to Judaism,
not only in Taif but elsewhere. Interesting in the highest degree is a
verse ascribed to Sakhr al-Ghay in the HodhaUian Poems, ed. Kose-
garten 18, 11. A thundercloud is there described, the centre of which
is an impenetrable mass ; only on the outer fringe a restless motion is
discernible. "Its fringes on the mountain-ridge (al-MalA) are like
Christians celebrating a banquet when they have found a Hanif, (and
so mn to and fro in the restlessness of glad excitement)."
■• ° Of course any one cnn read in a vision. Tlco question discussed
even by Moslems, as to whether the Prophet could read or not, has at
least DO place in this connexion.
548
MOHAMMEDANISM
[MOnAifMKD.
" Read I in the namo of tliy Lord, who created, created man from
a drop. Read I for thy Lord is the Most High wlio hath taught
hy the pen, hath taught to man what lie knew not. Nay truly
man walkcth in delusion, when ho deems that he suffices for him-
self; to thy Lord they must all return."
^yllat is Lere recorded is the commencement, not of
Mohammed's knowledge, but of his prophesying. That
the latter was due to a vision experienced by him on a
night of the month Ramadan (sur. xcvii. 1, ii. 181:) is
certain, and it is at least very possible that the form of
the vision was governed by the traditional conception of
revelation and prophecy which Mohammed had learned to
accept.^ It is, of course, uncertain whether the words in
which the angel called the Prophet are really contained in
sur. xcvi. Certainly this siira is very early, and its con-
tents are, indeed, the best expression of the original ideas
of Islam. Man lives on content with himself, but he must
one day return to his Creator and Lord, and give account
to him. This is in a sense the material principle of the
oldest faith of Lslam ; the formal principle is the very pro-
minent doctrine of revelation in writing copied from the
leavenly book.
When the angel left him — so the tradition runs on-^—
Jtohammed came to Khadija and recounted the occurrence
to her in much distress ; he thought that he was possessed.
She however comforted him, and confirmed him in the belief
that he had received a revelation and was called as a mes-
senger of God. . Yet his doubts returned, when there ensued
a break in the revelation, and they reached a distressing
height. He was often on the point of seeking death by
casting himself down- from Mount HirA. It is usuaDy
assumed that this state of anguish lasted fron. two to three
years. Then the angel is said to have suddenly appeared
a second time ; he came to Khadija in great excitement
and said : "Wrap me up ! wrap me up !" This, it must
be explained, was done when he fell into one of his swoons ;
and on this occasion, as often thereafter, the revelation
came during an attack. Then was sent do^vn siira Ixxiv.
beginning with the address — "O thou enveloped one!"
Henceforth there was no interruption and no doubt ; the
revelations followed without break, and the Prophet was
assured of his vocation.
That Mohammed did pass through many doubts and
much distress before he reached this assurance,, may well
be believed (siu*. xciii. '3) ; but the systematic development
Tlio of the doctrine of the fatra, or interval of from two to
fati-a. three years between the first and second revelation, belongs
to a later stage of tradition. It appears that it was . de-
vised to dispose of the controversy whether Mohammed
lived as a proj)het in Mecca for ten or for twelve years ;
perhaps, too, it was desired to solve another difficulty —
viz., whether sur. xcvi. or sur. Ixxiv. was the beginning
of the revelation — in a sense that should do some justice to
the rival claims of each.- The tradition may also have
been influenced by the circumstance that Mohammed, in
the first three years of his mission,' did not appear as a
public preacher,^ but only sought recruits for his owii cause
and the cause of All.'di in private circles. First, he gained
the inmates of Iris own house, — his wife Khadija, his xreed-
> 11. Dodwell, " De Tabulis colli," in Fabricius, Corf, psetid. V. T.,
2d cd., ii. 651 sq. Compare, in the Koran, especi.illy sur. IxJtxvii. 6,
"We will cause thee so to read that tliou inaycst forget nothing save
•what God mil." The following progress is noteworthy : — Isaiah's lips
arc touched to purge them of sin (Isa. vi. 7); Jeicmiah's are touched
hy the Lord to put His word in his mouth (Jer. i. 9) ; Ezckiel receives
the revelation as a roll of a hook which he lias to swallow ( Ezck. iii. 2).
= See Sprcnger in Z.D.M.O., 1859, p. 173 sq.; Noldeko, op. cIL,
67 sq. Ewald thinks that the vocatives at the beginning of sur. lixiv.
and Ixxili. mean simply — 0 long sleeper ! Tliis view is worthy of
consideration. Tlie Moslem cxcgetes thoroughly understand the art
of giving to general expressions of the Koran B])ecilic reference to
historical events wluch they have themselves invented to facilitate
'6XC£C3is. * Ihu Hishani, p. 160.
man TaxH b. Haritba, his cousin 'Ali (of who.se nurture he First
had relieved Abii Tdlib, a poor man with many children), <-onvert»-
and finally his dearest friend Abiibekr b. Abi KohAfa. '
The last named won for him several other adherents :
'OthmAn b. 'AffAn, Zobair b. al-'Aww4m, 'Abd al-Puilmian
b. "Auf, Sa'd b. Abi WakfeAs, Talha b. "Obaid AUAh, aU
names of note in the subsequent history of Islam. Soon
there was a little community formed, whose members united
in common exercises of prayer.
To the Hanff.s, especially to the family of Zaid b. 'Amr, '
their relation was friendly ; they had the name of iloslem
in common, and there was hardly any difference of prin-
ciple to separate them. The personality of the prophet
had given an altogether new impulse to a movement already
in existence ; that was aU. To found a new religion was
in no sense Mohammed's intention ; what he sought was
to secure among his people the recognition of the old and
the true. He preached it to the Arabs as Moses had before
him preached to the Je^s, and Jesus to Christians; itwaa
all one and the same religion as written in the heavenly
book. The differences between the several religions of the
book were not perceived by him till a much later period.
It is not difficult to understand why Mohammed should
in the first instance have turned- to those who were most
readily accessible to him ; but the nature of his mission did
not stiffer him to rest content with this ; it compelled him
to make public proclamation of the truth. One of hi:J
dependents, Arkam b. Abi Arkam, offered for this purpose
his house, which stood close by the sanctuary, and thus the
Moslems obtained a convenient meeting-place within the
town, instead of, as hitherto, being compelled to resort to
ravines and solitary places.^ Here Mohammed preached,
and here too it was that he received some converts to
Islam. But he did not'bbtain any great results among the
Meccans. 'WTiat he had to say was already in substance
familiar to them ; all that was new was the enthusiasm
with which he proclaimed old truth. But this enthusiasm
failed to make any impression on them ; they set him aside
as a visionary, or as a poet, or simply as one possessed.
In their eyes it was a fatal flaw that his supporters were
drawn from the slave-class and the lower orders, and the
ranks of the young ; it would have been quite another
matter if one of the rulers or elders had beUeved in him.
This circumstance was a source of annoyance to the pro-
phet himself ; in sur. Ixxx. we find him rebuked by God
for having repulsed in an imkind way a blind beggar who
had interrupted him as he was endeavouring to win over a,
man of influence — an endeavour which proved of no avail.
This indifference of the Meccans embittered the mes-
senger of God, and led him to give to his preaching a
polemical character which it had not hithcno possessed.
In the oldest suras we have monotheism in its positive and
practical form.' God is the all-powerful Lord and all-know-
ing Judge of man ; ho demands loyal self-surrender and
unconditional obedience ; the service he requires is a serious
life, characterized in particular by prayer, almsgiving, and
temperance. That the worship of other gods beside AUAh
is excluded by these views, goes without saying ; still it i«
* It does not apjwar that Arkam 's house was of the nature of an
asylum to which Mohammed betook himself for refuge from the ill*
treatment to which ho was subjected in his own home, nor is tlierfl
any evidence that ho ever lived m it. It w,is simply the meeting-
house of the oldest Islam. Prayer continued to bo olTered within it
until the conversion of 'Omar, who was hold enough to choose thq
Ka'ba itself, the centre of heathenism, as the Moslem place of prayer,
Comp. Muir, ii. p. 117 ; Sprcnger, i. p. 434.
' V.nmt is meant by practical monotheism is most easily understood
by reference to Matt vi. 24 sqq.^ x. 28 sqq., and to Luther's exposi-
tion of the first commandment in the catechisms ; it is the essence of
religion. We do not, of course, mean that this practical monotheism
is expressed in the Koran with as mucli purity and depth as in tli«
GospcL
■ilOHAJXilED.]
MOHAMMEDANISM
549
noteworthy that the chp.i-p Bc^ations of monotheism ac-
quired prominence only by degrees. It was in his indig-
nation against the cold mockery with which he was met
that Mohammed first assumed an attitude of hostility
towards the worship of polytheism, while at the same time
he gave much greater prominence to his own mission, just
because it was not acknowledged. He now began to
threaten the infidels with the judgment of God for their
contempt of His message and His messenger ; he related
to them the terrible punishments that in other cases had
fallen on those who refused to hear the voice of their pro-
phet, applying the old legends to the circumstances of the
present with suth directness that it was superfluous ex-
Hostilitj- pressly to add the morals. This could not fail to irritate
of the tlie Meccans, especially as after all the new religion gained
Meccans. gro\iud. What Mohammed attacked as ungodly and abom-
inable were their holy things ; they were jealous for their
gods and their fathers. Their attachment to the tradi-
tional worship was the greater that the prosperity of their
town rested upon it ; for they had not yet learned that the
Ka'ba was no institution of heathenism. They found, how-
ever, no other way to remo'i'e the public scandal than to
approach Abii T41ib, the Prophet's uncle and the head of
his family, asking him to impose silence on the offender,
or else to withdraw from him his protection. Ab\i T^lib
was not personally convinced of Mohammed's mission, but
he did not choose to impose conditions on the enjoyment
of his protection. -Ait length, however, when the Meccans
adopted a threatening tone and said that he must either
restrain his nephew from his injurious attacks, or openly
take side for Mohammed and against them, he sent for his
nephew, told him how things stood, and urged him not
to involve them both in ruin. Mohammed was deeply
moved ; he thought his uncle wished to get rid of him ; yet
he could not and would not withdraw from the divinely-
imposed necessity which impelled him to preach his con-
victions. "Though they gave me the sun in my right
hand," he said, " and the moon in my left, to bring me
back from my undertaking, yet will I not pause till the
Lord carry my cause to victoi-y, or till I die for it." AVith
this he burst into tears, and turned to go away. But
Ab\i TAlib called him back and said : " Go in peace, son of
my brother, and say what thou wilt, for, by God. I will on
no condition abandon thee.".
The protection of his uncle did not relievo Mohani'ctied
from all 'manner of petty insults which he had to endure
from his enemies from day to day; but no one ventured to
do him serious harm, for the family feud which this would
necessarily have produced was not to be lightly incurred.
Less fortunate than the Prophet, however, were such of
his followers as occupied dependent positions, and had no
family support ; especially the converted bondmen and
bondwomen, who found no consideration, and were often
treated with actual cruelty. For some of these Abi'ibekr
purchased freedom. There seem to have been no martyrs,
but the situation of many Moslems became so intolerable
that they fled to Abyssinia. The Abyssinian Christians
were quite looked upon as their religious kinsmen.
The torn- A breach \vith one's people is for the Arab a breach with
por.iry Gtod and the ■world ; he feels it like a living death. Mo-
conipro- iiajnmed, who remained in Mecca, naturally made every
efi'ort to heal the breach with his to^vnsmen, and, as natur-
ally, the latter met him half-way. He even went so far
as to take the edge from his monotheism. Once, when
the heads of the Koraish were assembled at the Ka'ba,
Mohammed, we are told, came to them and began to recite
before them sur. liii.' When he came to the passage,
^ Tlie authorities for tliis are Ibu Sa'd, tlie secretary of WakiUi, to
■whom we owe the preservation of Wakiili's materials for the .^reccan
period, and especially Tahari; comp. Muir, ii. 150 sqq. Tiie comninn
"What think ye of al-LAt and al-'Ozz.d, and of Manit the
third with them?" the devil put words in his mouth which
he had long wished to have by revelation from God — viz.
" These are the sublime Cranes,^ whose intercession may
be hoped for." The auditors were surprised and delighted
by this recognition of their goddesses, and when Mohammed
closed the stira with the words, " So prostrate yourselves
before AlUh and do service to him," they all with one
accord complied. They then professed their satisfaction
with his admissions, and declared themselves ready to
recognize him. But the messenger of God went home dis-
quieted. Li the evening Gabriel came to him, and Mo-
hammed repeated to him the stira ; whereupon the angei
said: "What hast thou done? thou hast spoken in the ears
of the people words that I never gave to thee." Mohammed
now feU into deep distress, fearing to be cast out from the
sight of God. But the Lord took him back to His grace
and raised him up again. He erased the diabolical verse
and revealed the true reading, so that the words now ran —
" What think ye of al-LAt and al-'Ozzi, and of Man.-it the
third with them? The male [offspring] for you and the
female for Gfod ? ' That were an unjust division ! " Wheii
the new version reached the ears of the Meccans they
compared it with the old, and saw that the Prophet had
broken the peace again. So their enmity broke out again
with fresh violence.
It is generally and justly suspected that this compromise
did not rest on a momentary inspiration of Satan, but was
the result of negotiations and protracted consideration.
Nor was the breach so instantaneous as is represented ;
the peace lasted more than one day. There is no doubt
as to the fact itself. Every religion must make compro-
mises to gain the masses. But for Mohammed the moment
for this had not yet arrived ; later on he tised the method
of compromise with great effect.
The news of the peace between Mohammed and the
Meccans had recalled the fugitive Moslems from Abyssinia ;•'
on their return the actual state of affairs proved very
different indeed from what they had been led to expert,
and it was not long before a second emigration took plai ■•.
By degrees as many as a hundred and one Moslems, mostly
of the younger men, in little groups, had again migrated
to Abyssinia, where they once more met with a friendly
reception. Among them were Ja'far, the brother of 'Alt,
and the Prophet's daughter Rokaj'ya, along with her hus-
band 'Othmin b. 'Affan.*
Mohammed's position was very considerably altered for
the worse, both subjectively and in other respects, by his
precipitate withdrawal from the compromise almost as soon
as it had been made. He himself indeed, although long
and salutarily humbled by the remembrance of his fall
(sur. xvii. 75 sqq.), never abandoned faith in his vocation ;
his followers also did not permit themselves to be led
tradition ignores the fact itself, Init knows it5 i-esult, the retnru of the
Abyssinian fngitives.
= " Al-gharHnlk al-'M" fino-soundiiig but perliap.i meaningless
words— „ jjcrrlicli, et^-as donkel zwor.
DocU es kliiigt reclit wunderbar."
Comp. Ndldcke, op. cit., p. 80. Hobal, thoiiK'i the chief god of the
Meccans, is not mentioned in the Koran cither Iierc or elsewhere.
Perhaps as God of the Ka'ba he w.is already identified with Allah by
the Meccans, or was so identified by Mohammed.
' The date assigned is the month Rajab of the fifth year of the Call,
corresponding to the eighth ye.ar before the Flight (a.d. 814-615).
The compromise must have been made in the interv.al. The chronology
of this period is of course in the highest degree uncertain, and the
order of the events hard to ascertain. Thus it can srarcely be deter-
mined whether the above-mentioned scene with Abu "Talib ought to be
placed before or after the compromise.
* 'Othmiln and Eokayya, hwcvcr, members of the noble house of
Omayya, soon returned, along with many othi rs. TIic rest remained
in exile until the seventh year of the Flight.
650
MOHAMMEDANISM
[moha^oikd.
away. But thb M^ccans, from the way in'which he .had
at first given out a verse as God's word and afterwards
withdrawn it as a suggestioH of Satan, did not hesitate to
draw the inference that the whcile of his boasted revelation
was nothing but a manifest imposture. To their cold and
unfeeling logic the Prophet had nothing to oppose save
passionate assurances.
VTaniM Fortunately for the Moslems, precisely at this juncture,
aud when matters were assuming so gloomy an aspect for their
Oinor. little company, two conversions took place, which were well
fitted to revive their coiurage. ISIohammed's uncle, Hamza
b. 'Abdalmottalib, felt his family pride wounded by the
injurious treatment which the former had received from
Abu Jahl, head of the great and wealthy family of the
Banii Makhziim, and in order to become publicly his
champion, he adopted Islam. Of touch more importance
still was the conversion in the same year (the sixth of the
Call) of "Omar b. al-KhatUb. 'Omar was then only twenty-
six j'cars of age, and neither rich nor noble ; but his im-
posing figure and his unbending strength of will gave him
a personal influence, which immediately made itself felt in
a very marked manner in favour of Islam. Until now its
religious gatherings had taken place privately, especially
in the house of Arkam ; but 'Omar offered his prayers at
the Ka'ba as publicly as possible, and his example was
followed by the other Moslems. Their religious exercises
were no longer gone about in secret, but ostentatiously
and before the eyes of all.
So far as can be gathered, it was at this time that the
opposition between Mohammed and his townsmen r6ached
its highest pitch. The feeling that he had somewhat
committed himself embittered him ; he was determined to
atone for his previous concessions to polytheism by un-
compromising polemic against it. A personal element,
which had lurked from the first in the war of principles,
became by degrees increasingly dominant. The idols were
less displeasing to Allih than the idolaters ; his own wor-
ship was a matter of less concern to him than the recogni-
tion of his messenger. With ever-increasing distinctness
the prophetic utterances came to be mere words of threaten-
ing and rebuke against the Meccans; it was impossible
not to recognize in Noah and Moses or Abraham the pro-
phet himself. The coming judgment upon Mecca, and the
hour of it, were either in plain words or veiled allusion
the continual theme of the " admonisher ; " but the oftener
and the more urgently it was repeated, the less vras the
impression it produced. The Meccans did not, on the
whole, suffer themselves to be much disturbed by the pro-
spect of the terrible overthrow which was portrayed before
them in vivid colours. They were even profane enough
to express a desire to see the long-threatened catastrophe
arrive at last, and their audacity went so far as to complain
of the revelations with which Mohammed sought to stir
their feelings as being tedious.^ They did not in the least
believe that the Biblical narratives, which he related with
special pride, were known to him by revelation ; on the
contrary, they pretended to know perfectly well the human
source from which he had derived them (sur. xvi. 105 ;
XXV. 5; xliv. 1.3). It is very interesting to find Mohammed
in presence of their unbelief referring to the recognition
and approval mth which he met among the children of
Israel (sur. vi. 114; x. 94; xiii. 36 sqq.; xvii. 108; xxviii.
52 sq.; xxxiv. 6), and particularly to find him appealing
to the testimony of a certain Jew, whom he does not name
(sur. xlvi. 9 sqq.) Manifestly he had relations with .Jews
at this period, and was under their influence ; and from
them, of course, it was that the material of his Old Testa-
ment and Haggadistic narratives was derived. At the
' Ibn Hisbira, pp. 191, 235 54.
same time it is clear that he himself must have believni
these to have come directly to him in a second revelatiua
from above, otherwise he v/ould hardly have taken his'
stand in the presence of his opponents upon the testimony
of the Jews. Such a self-deception seems indeed hardly
credible to us, but it is impossible to impute to the Arab
prjphet too complete an absence of the critical faculty.
The KoraLsh at last lost all patience. Their heads The In-
entered into a solemn compact to break off all intercoiu-.'-.e tcdict.
with the Hashimids, as they declined to separate them-
selves from Mohammed. The Hashimids submitted to
the interdict for the sake of their relative, although for
the most part they were not believers on him. Along
with the Banii '1-Mottalib they withdrew into the separate
quarter of their chief, into the so-caUed Shi'b Abi Tilib ;
one only of their number, Abti Lahab, separated himself
from them, and made common cause with the Meccans.
All buying and seUing with the excommunicated persons
being forbidden, these found themselves reduced occasion-
aDy to outward distress, as well as excluded frcsa all
fellowship. This treatment, although apparently jiever
carried out with absolute strictness, did not fail of its
effect. The Prophet's more remotely attached adherents
fell away from him, and his efforts for the spread of Islam
were crippled. All he could do was to. encourage those
who remained faithful, and to set himself to seek the con-
version of his relations.
This state of matters, after continuing for from two to
three years, at last became intolerable to the Meccans
themselves, who had a variety of relations with the ex-
communicated family. In the tenth year of the Call (a.d.
619-620) five of the leading citizens paid a visit to the
Shi'b Abl X^lib and induced the Banil HAshim and al-
Mottalib to come out of their retirement and again appear
among their fellow-citizens. The rest of the Koraish were
taken by surprise, and did not ventiu-e, by setting them-
selves against the fait accompli, to run the risk of what
might have become a dangerous breach. The story goes
that a lucky accident released them from the solemn oath
under which they had laid themselves with reference to the
Banii HAshim — the mice had destroyed the document,
hung up in the Ka'ba, on which it was recorded.
Mohammed was now free once more ; but he no longer IT:* Pro;
thought of carrj'ing on his polemic against the Meccans orP*"''
of seeking to influence them at all. In his relations to ^J[
them three stadia can be distinguished, although it is easier
to determine their character than their chronology. In
the first instance, his endeavour was to propitiate them
and win them over to his side ; when other methods failed,
he even went so far as to make complimentary mention o€
their goddesses in one of his revelations, and thus to set
up a compromise with heathenism. When this compromise
failed, he forthwith commenced an embittered assault upon
the idolaters, which ended in the outlawry of himself and
of his family. And now, the ban having been removed,
he gave the Meccans up, abandoning them to their hard-
ness of heart. It had become clear to him that in his
native town Islam was to make no progress, and that his
position was untenable. His feeling of separation was in-
creased all the more ivith the death of his faithful Khadija
about this time, followed soon afterwards by that of Abti
Talib, his noble protector. He accordingly came to the
determination to take his chance in the neighbouring T^if, Visit
and set out thither alone. On his arrival he asked theT»'^
heads of the town whether they would be willing to receive
him and protect the free proclamation of his doctrines.
He was answered in the negative ; the mob drove him out
of the town, a^d pursued him until he found refuge in a
vineyard, the property of two noble Meccans. In the
deepest despondency ho again took the homeward road.
'MOBAMMEO.'I
MOHAMMEDANISM
551
Tradition has it that he found comfort in the fact that at
I'^ast the Jinns listened to him as by the way he chanted
the Koran in the sacred grove of Nakhla.' In the present
circuiastances it was now impossible for him to return into
the town, after having openly announced his intention of
breaking with it and joining another community. He did
not venture to do so until, after lengthened negotiations,
he had assured himself of the protection of a leading citizen,
Mot'im b. "Adt Notwithstanding all that had happened,
he resolved, two months after the death of Khadfja, to enter
upon a second marriage with Sauda bint Zam'a, the widow
of an Abyssinian emigrant.
Chance scon afterwards brought to pass what fore-
thought (on his journey to T^if) had failed to accomplish.
After having given up the Meccans, Mohammed was wont
to seek interviews with the Arabs who came to Mecca,
Majanna, Dh\i '1-MajAz, and 'Ok4z, for the purpose of taking
part in the feasts and fairs, and to preach to them.' On
one such occasion, in the third year before the Flight
The men (a.d. 619-620), he fell in with a small company of citizens
of Me- of Medina, who to his delight did not ridicule him, as was
^*- usually the case, but showed both aptness to understand
and willingness to receive his doctrines. For this they
had been previously prepared, alike by their daily inter-
coiirse with the numerous Jews who lived in confederation
with them in their town and neighbourhood, and by the
connections which they had with the Nabatseans and
Christian Arabs of the north. Hanifitism was remarkably
■widely diffused among them, and at the same time there
•were movements of expectation of a new religion, perhaps
even of an Arabian Messiah, who should found it. Medina
was the proper soil for Mohammed's activity. It is singular
that he owed such a discovery to accident. He entered
into closer relations with the pilgrims who had come from
thepce, and asked them to try to find out whether there
was any likelihood of his being received in their town.
They promised to do so, and to let him hear from them in
the following year.
At the pilgrim feast of next year, accordingly, twelve
citizens of Medina had a meeting with Mohammed,' and
gave him their pledge to have no god but AH&h, to with-
hold their hands from what was not their own, to flee for-
nication, not to kill new-bom infants, to shun slander, afd
to obey God's messenger as far as was fairly to be asked,*
Fi«t This is the so-called First Homage on the 'Akaba.* The
Homnge twelve men now returned, as propagandists of Islam, to
"\kaba. '^^''^ homes with the injunction to let their master hear
of the success of their efforts at the same place on the
following year. One of the Meccan Moslems, Mos'ab b.
'Omair, was sent along with or after them, in order to teach
the people of Medina to read the Koran, and instruct them
in the doctrines and practices of Islam.
Islam spread very quickly on the new soil. It is easy
to understand how his joy strengthened the Prophet's
spirit to try a higher flight. As a symptom of his exalted
frame we might well regard his famous night-journey to
Jerusalem (sur. xvii. 1 ; vi. 2), if we could be sure that it
■ Sur. idvi. 28 ; liidL 1. On tUe impossibility of historically fining
the date of this occurrence see Noldeke, op. cit., p. 101.
' Muir (ii. 181 s;.) assumes, with good reason, that he had already
done so during the time when he was living in the Shi'b Abi Tdlib,
and assigns to this period the story that Abii Lahab followed liim in
this in, order to counteract his preaching, and sow tares among the
wheat.
* Sprenger (ii. 526) identifies this meeting with the first, which tra-
dition distinguishes from it and places a year earlier. He is probably
'right
* Afterwards this was called the women's oath. It is a noteworthy
summary of the features by which Islam is distinguished from
heathenism.
* On the 'Akaba compare Vakidi, pp. 417, 427, 429. It ww s
tatioa between 'Arafa and Mind.
belonged to thi.i period.' The prophecy also of the final
triumph of the Romans over the Persians (contained iu
sur. XXX. 1 sqt].) might very well pass for an expression of
his own assurance of victory, as at that time he still had a
feeling of solidarity with the Christians. But the prophecy
(the only one contained in the Koran) belongs, it would
appear, to a much earlier date.''
At the Meccan festival of the last year before the Flight
(in March 622) there presented themselves among the pil-
grims from Medina seventy-three men and two women who
had been converted to Islam. In the night after the day of
the sacrifice (hey again had an interview with the Projiliet
on the "Akaba ; AJ-' Abbas, his uncle, who after Abi\ fdlib's
death had become head of the Banii HAshim, wa-s also Second
present. This is the so-called Second Homage on the Homagt
"Akaba, at which Mohammed's emigration to Medina was
definitely settled. Al-'Abbis solemnly transfentd his
nephew from under his own protection to that of the mtn
froin Medina, after these had promised a faithful dischargo
of the duties this involved. 'They swore to the Prophet to
guard him against all that they guarded their wi\ cs and
children from. He, on the other hand, promised thence
forward to consider himself wholly as one of themselves,
and to adhere to their society. According to the tradition
this remarkable scene was brought to a close by a sudden
noise.
The Meccans soon got wind of the affair, notwithstand-
ing the secrecy with which it had been gone about, but
Ibn Obay, the leader of the Medina pilgrim caravan, whom
they questioned next morning, was able wth good con-
science to declare that he knew nothing at all about it, as,
being still a heathen, he had not been taken into the con-
fidence of his Moslem comrades, and he had not ob.«erved
their absence over night. The Meccans did not gain
certainty as to what had occurred, until the men of Medina
had left. They set out after them, but by this they gained
nothing. They next tried, it Ls said, violently to jirevent
their own Moslems from migrating. After a con.-'idei-able
pause, they renewed the persecution of the adherents of
the Prophet, compelling some to apostasy, and shutting up
others in prison. But the measures they adopted were in
no case effective, and at best served only to precipitate the
crisis. A few days after the homage on the 'Akaba,
Mohammed issued to his followers the formal command to
emigrate. In the first month of the first year of the The emi-
Flight (April 622) the emigration began ; within two eration.
months some 150 persons had reached Medina. Apart
from slaves, only a few were kept behind in Mecca.*
Mohammed himself remained to the last in Mecca, in the
company of Abiibekr and 'All. His reason for doing so is
as obscure as the cause of his sudden flight. The explana-
tion offered of the latter is a plan laid by the Meccans for
his assassination, in consequence of which he secretly
withdrew along with Abtlbekr. For two or three days the
two friends hid themselves in a cave of Mount "Thanr,
south from Mecca, till the pursuit should have passed
over (sur. ix. 40). They then took the northward road
and arrived safely in Medina on the 12th of Eabf of the
first year of the Flight.' Meanwhile, 'AH remained three
■ See Muir, ii. 219 sqq. ; Sprenger, ii. 527 sqq- ; and on the other
side, Noldeke, Koran, p. 102. The masrH was afterwards called
mir&j (ascension), and, originally represented as a \ision, came to bo
regarded as an objective though instantaneous occurrence.
' See on the one hand Muir (ii. 223 sqq.) and Sprenger (ii. 527 SJ7.),
and on the other Noldeke (Qoran, p, 102; Taburi, p. 298). The
manner in which Sprenger seeks to make the prophecy a vaticlnium ex
evcntu is unfair,
^ Ibn Bisham, pp. 315 sq., 319 sq.
' The 12th of Rabi' is, according to tradition, the Prophet's birth-
day, the day of his arrival in Sledina, and the day of his death. It
is certain that he died at mid-day on Monday tlia 12th of Babf, but
552
days longer in Mecca, for the purpose, it is alleged, of
restoring to its owners all the property which had been
entrusted for safe keeping to the Prophet. The Koraish
left him entirely unmolested, and threw no obstacle in the
way when at last he also took his departure.
. With the Flight to Sledina a new period in the life of
the Prophet begins ; seldom does so great a revolution
occur in the cii-cmnstances of any man. Had he remained
in Mecca he would in the best, event have died for his
doctrine, and its triumph would not have come until after
his death. The Flight brought it about that he, the
founder of a new religion, lived also to see its complete
victory, — that in his case was united all that in Christen-
dom is separated by the enormous interval between Christ
and Constantine. Ho knew how to utilize Islam as the
means of founding the Arabian commonwealth ; hence the
rapidity of its success. That this was of no advantage for
the religion is easily understood. It soon lost the ideality
of its beginnings, for almost from the first it became
mixed up with the dross of practical considerations. In
reaching its goal so soon its capability of development was
checked for all time to come ; in every essential feature it
received from Mohammed the shape which it has ever
since retained. It onght not, however, to be overlooked
that the want of ideality and spiritual fmitfulness was
partly due to its Arabian origin.
Mohammtd in the first instance took up his quarters in
the outlying village of KobA, where several of his most
zealous adherents had their homes, and had already built
a mosque. It was not until after some days had passed,
and he had made himself sure of the best reception, that
he removed to the city itself, which at that time bore the
name of Yathrib. All were anxious to have him ; in order
that none might feel themselves slighted, he left the de-
cision to the camel (al-Kaswa) on which he rode. It
knelt down in an open space in the quarter of the Bauii
NajjAr, which he accordingly selected as the site of the
mosque and of his own house. At first he took quarters
for seven months in the house of Abii Ayyi5b ; within this
interval the juosque was finished, which was to serve at
once as the place of religious gatherings and as the com-
mon hall. Close to it was the Prophet's pi'ivate dwelling,
consisting of the huts of his wives, in one or other of
which he lived. At that time he had only one wife, the
Sauda already mentioned ; but soon he married, in addi-
tion, the youthful 'Aisha, the daughter of his friend
Abubekr, who acquired great influence over him. Some
of the leading emigrants built houses in the same neigh-
bourhood, while the test continued to be quartered with
the jicople of Medina.
]\Iedina is situated on a westward spur of the Arabian
tableland, on the Wadi KanAt. It is an oasis amongst
barren rocks, mostly of volcanic origin. The inhabitants
su]iported themselves by their date palms and by the field
and garden fruits tliat grew under their shadow ; they had
thtlr homes partly in the town itself and partly in the
suburbs and outlying villages. At one time the oasis had
belonged to the Jews, as the similar oases to the north
still did— Wadi 'l-Kori, Khaibar, Fadak, Taimi. But
some centuries befoic Mohammed's time, Arabs of Yemen,
the Banii Kaila, had immigrated and partially driven the
Jews away. Many Jews, however, still continued to live
there, partly scattered among the Arab tribes and under
their protection, partly also in independent communities
such as the KainokA, the Nadir, and the Koraiza. For
them it was a great advantage that the Arabs were not
agreed among themselves. The Banil Kaila were divided
MOHAMMEDANISM
[MOHAJtirXD.
' the olliftr xtttfrneiils Are all tlio mope suspicions because tliey also
•peal! of Monday aud mid-day. Comp. Niildclic, Qoran, p. 69 tj.
into two branches, the Aus and the Khazraj, who were Acs md
constantly at daggers drawn. The mutual hate which Khunj.
burned within them, from time to time manifested itself in
murder and assassination, if by any ahance one of the Au3
had wandered into a Kliazrajite quarter, or wee versd.
Shortly before the arrival of Mohammed, the battle of
Bo'Ath had taken place within the liberties of Medina, in
which theAusJ with the help of their Jewish allies, had
vanquished the IChazraj and broken their preponderance.
The Khazraj were the more numerous and powerful, and
seem to have been on the point of making their leading
man, Ibn Obay, the king of Medina; by the battle of
Bo'dth the balance of parties — and anarchy — was pro-
served in the interests of a third, who came in at the right
moment to settle these <'»rible and exhausting feuds and
restore order.
The circumstances were singularly fitted to change the 5io»«ni-
religious influence which Mohammed brought along with '"«<''» 1»
him into another of a political character, and from being a •.\"'™."**
prophet to make him the founder of a commonwealth. The ' ' """
Arabs had hitherto been accustomed to lay before their
Kihins, or priestly seers, at the sanctuaries, for decision in
God's name, all sorts of disputes and hard questions which
ordinary means were inadequate to decide. The religious
prestige which Mohammed enjoyed led directly to his
being frequently called in as ad-viser and judge. In
Medina quarrels and complications were abundant, and an
authority to stand over both parties was much needed.
Mohammed met this need in the manner which was most
acceptable to the Arabs ; the authority he exercised did
not rest upon force, but upon such a vohuitary recognition
of the judgment of God as no one had any need to be
ashamed of.' In principle, it was the same kind of judicial
and public influence as had been possessed by the old
KAhins, but its strength was much greater. This arose
not only from the peculiarly favourable circumstances, but
above aU from Mohammed's own personality. It is im-
possible to understand the history until one has mastered
the fact of his immense spiritual ascendency over the
Arabs. The expedient of giving oneself out for the mes-
senger of God, and one's speech as the speech of God, is
of no avail to one who finds no credence ; and credence
such as Mohammed received is not given for any length of
time either to an impostor or a dupe. Even the respect
in which he was held as a prophet would have helped him
little if his decisions had been foolish and perverse. But
they were in accordance with truth and sound understand-
ing; he saw into things and was able to solve their riddle ;
he was no mere enthusiast, but a thoroughly practical
nature as well.
It was not long before he was able to demand as of right
ihat which, in the first instance, had been a voluntary tri-
bute. " Every dispute which ye have one with another
ye shall bring before God and Mohammed ; " so runs the
text in the original constitution for Medina, set up in the
first years after the Flight-; and in the Koran a rebuke is
given to those who continue to seek the administration of
justice at the hands of the false gods, i.e. of their priests
and seers.' With incredible rapidity the Prophet as a
veritable "liAkim biamr Alhih" had come to be the most
powerful man in all Medina.
*^ Very significant if* it that the Moslems were ready to submit even
to puni;^imunt with stripes, if aw.arded by God.
2 Ibn HLOiam, 342, 17.
' Ibn Hishira, 360, 8 sqq. Jolis b. Sowiiid and other hypocrites
were summoned before Mohammed by their believing relatives on Re-
count of some dispute ; but they in their turn summoned the plainlitl's
before the Kiiliius, who in the days of heathenism had bsen tltcir
judges. It was with reference to this that sur. iv.' 63 was revealed —
" Hast thou not tAkcn note of those who profess to be believer.^, yet
wish to carry on their suit before the false gods 1"
•lOHAMSIlO).]
M O H A M M E D A N I S 31
553
Moliammed thxxa laid the foundations of his position in
a manner precisely similar to that which Moses (Exod.
xviii.) is sjiid to have followed ; and jast as the Torah grew
oat of the decisions of Moses, so did the Sunna out of thoss
of Mohammed. It was perhajis in judicial and regulative
activity, which he continued quietly to carry on to the
very end of his life, that his vocation chiefly lay. At all
events his work in this direction was extremely beneficial,
if only because he was the creator of law and justice where
previously there had been nothing but violence, self-help,
or at best voluntasy arrangement. But the contents of
his legislation also (if it can be called by such a name)
marked a distinct advance upon what had been the previ-
ous use and wont in Arabia. In particular, he made it
|iis special care to set a fence round the rights of property,
and to protect and raise the place of woman in marriage.
Blood revenge he retained indeed, but completely altered
its character by reserving to himself the right of permitting
it ; in other words, the right of capital sentence. It need
not be said that in many ways he availed himself of th;.:
■vvliich already existed, whether in the form of Arab uso;'
or of Jewish law ; he followed the latter, in particular, it
his laws relatijig to marriage.
1. The new situation of afiFairs inevitably brought it abo'a'
that religion was made a mere servant in the work of
forming a commonwealth. Xever ha-s this service been
better performed ; never has it been utilized with greater
adroitness as a means towards this end. In Mecca, Islam
had originally been nothing more than the individual con-
viction of Mohammed ; it was oidy after severe struggles
that he went so far as to preach it, and even his preaching
lad no other aim than to create individual conviction in
others. What he said was of the simplest description —
that people ought to believe in God and in judgment to
come, that men ought to live their lives seriously and not
Avastc them in f allies, tliat one ought not to be high-minded
or covetou-s, and so on. A community arose, it is true,
c\en in Mecca, and was confirmed by the persecutions.
There also religious meetings were held and social prayers.
l!ut everything was still in a very fluid and rudimentary
stage ; religion retained its inward character. It was not
■until the first two years after the Flight that it gradually
lost this, and became, if not exclusively, yet to a very large
extent, a mere drill system for the community.* No god
but the one God (lA ilih ilia 'Uah) was the entire sum of
tlieir dogmatic, and less importance was attached to belief
in it than to profession of it. It was the watchword and
battle-cry. The prayers * took the form of military exer-
cises ; ihey were imitated with the greatest precision by
the congregation, after the example of the Im&m. The
mosque was, in fact, the great exercising ground of Islam ;
it was there that the Moslems acquired the esprit de cor»s
jjnd rigid discipline which distinguished their armies.
Next to the monotheistic confession (tauhiJ) and to
"prayer (salit) came almsgiving (zakAt, sadaka) as a third
important means by which Mohammed awakened and
brought into action among his followers the feeling of fellow-
ship. The alms by and by grew to be a sort of tithe, which
1 Tliia ia to be understood as appl\-ing to the system as a wliole.
Of course, there are always individuaU who break through systeai ;
tut the historical power of Islam rests upon the system. To the
■system also belongs the spiritual jargon which Mohammed introduced.
It was no longer permissible to say " Qood morning J ' ('im sabiilian),
the phraie now ran, " Peace be with thee ! " and on every occasion
pious fonns of speecli were demanded. Characteristic of the puritan-
ism of the system is tlie prohibition of wine and of gnming, first issued
im the yean immediately following the Fligiit, and the contempt for
poetry.
- They were five in number — at sunrise, noon, afternoon, sunset, and
late evening. E.icli pi-ayer consisted originally of two, afterwards of
"four, prostr-itions. The chief weekly public service (jom'a), with ser-
mon, was held on Friday at mid-Jay.
afterwards became the basis of the Jloslem fiscal system,
and so at the same time the material foundation of the
Moslem state. Religion received so practical a develoi>-
roent that of alms nothing but the name remained, and
the convenient fiction that the taxes had to be paid to God.
Just in proportion to the closeness of the union into
which Islam brought its followers did its exclusivene.ss
towards them that were without increase. If in Mecca
Mohammed in his relations to the other monotheistic reli-
gions had observed the principle, " ho that is not against
me is for me," in Medina his rule was " he that is not for
me is against me." As circumstances were, he had to ad
just matters chiefly with the Jews. Without any inteiition
on their pait, they had helped to prepare the ground for
him in Medina ; he had great hopes from them, and at Srst
treated them on no different footing from that of the Arab
families which recognized him. But as his relations with
the Aus and Khazraj consolidated, those which he had
with the Jews became less close. The conjunction of reli-
gious with political authority, the development of civil
polity out of religion, of the kingship from the prophetic
function, was precisely what they objected to.^ On tho
other hand, while the old polity of Medina, broken up and
disorganized as it was, had no difficulty in tolerating
foreign elements within its limits, the new political system
created by Islam changed the situation, and rendered it
necessary that these should be either assimilated or ex-
pelled.
Mohammed's hostility to the Jews found expression, in
the first instance, theoretically more than practically,* and
especially in the care with which he now differentiated
certain important religious usages which he had taken over
from Judaism, so that they became distinguishing marks
between Islam and Mosai.sm. Thus, for example, he altered
the direction of prayer (Kibla), which formerly used to ba
towards Jerusalem, so that it now was towards Mecca ;
and for the fast on the 10th of Tisri ('Ashiird) he sub^
stituted that of the month of Ramadan.* In apijointing
Friday as the principal day of public worship, he may also
possibly have had some polemical reference to the Jewish
Sabbath. Of these alterations the greatest in positive
importance is the transference of the Kibla to Mecca. It
symbolizes the completion of the Arabizing process which
went on step by step with the change Islam underwent
from being an individual to being a political religion. In
substituting the Meccan Ka'ba for the sanctuary at Jeru-
salem, Mohammed did not merely bid farewell to Judaism
and assert his independence of it ; w;hat he chiefly did was
to make a concession to heathenism, and bring about a
nationalization of Islam, for the purpose of welding togethei"
the Arab tribes (Kabiil) into one community. Of similar
.significance was the institution of the feast of sacrifice ('id
al-doh.A) on the day of the Meccan festival. The Moslems
were to observe the latter as much as possible, even if they
could not be actually present on the spot.
Thus we have the five chief precepts of Islam — (1) Con-
fession of the unity of God ; (2) stated prayer ; (3) alms-
giving; (4) the fast of Ramadan; (5) observance of the
festival of Mecca. Capable of having deeper meanings
crefls'd
ckIu
Tli«
Jews.
Precepts
of Isk.31
» While Islam had the effect of uniting the Arabs politically, uni-
formity of religion ui the case of the Jews had no such effect ; on tho
(-•ontrary, the mutual feuds and hatreds in wl'iich they indulged con-
duced greatly to the advantage of the Moslems. The Jews, of course,
recognised Mohammed's supremacy as a fact, but they denied .any legal
title thereto as arising from his prophetic office
* Comparo the well-known second siVra, in which a long attack is
made on Judaism. .
• A connection with the Christian fasU U usually alleged. It is
possible that Christian innacnc&may have to do with the loug duratiou
of the fasts, but it cannot have anything to do with the selection of I
Ramad.in ; for in the first years alter the Flight, KamnAm fill not ia )
* Spring but in December.
XVI. — - o
654
MOHAMMEDANISM
' [iiOHAlEfED.
attached to them, but meritorious also, even in a merely
external observance, they were an excellent instrumentality
for producing that esprit de corps, that obedience to Allih
and his messenger, which constituted the strength of the
Mosfem system. Up till that time blood-relationship had
been the foundation of all political and social relations in
Arabia ; upon such a foundation it was impossible to raise
any enduring edifice, for blood dissociates as much as it
unites. But now, religion entered upon the scene as a
much more energetic agent in building the social structure;
it ruthlessly broke up the old associations, in order to
cement the thus disintegrated elements into a, new and
much more stable system. The very hearts of men were
changed ; the sanctity of the old relationships faded away
in the presence of AllAh ; brother would have slain brother,
had Mohammed willed it. .The best Moslem was he who
was the most remorseless in separating from the old and
attaching himself to the new ; Mohammed gave preference
to active natures, even if they occasionally kicked over the
traces ; contemplative piety received from him only the
praise of words. Over the anarchical rule of a multi-
tude of families the sole sovereignty of God came forth
triumphant ; its subjects were united by the firmest of all
bonds. Every Moslem was every Moslem's brother, and,
SIS matter of course, took his part as against every non-
Moslem. Outside of Islam there was neither law nor
safety; AllAh alone was powerful, and he protected those
only who acknowledged his sole sovereignty.
Emi- 'rhe Emigrants (Moh4jira), who along with the Prophet
pants liad fled from Mecca, were the kernel and the cement of
and De. jjjg community. It was made all the easier for them to
give effect to the fundamental principle, that citizenship
in Medina depended not on family but on faith, because the
natives themselves (AnsAr, "the Defenders"), consisting of
Aus and Khazraj, neutralized one another by their mutual
enmity. Mohammed seems at first to have cherished the
design not only of entirely disowning relationship with
non-Moslems, but also of obliterating as much as possible,
within Islam, the distinctions of blood, by means of the
common faith. He established between emigrants and
individual citizens of Medina relationships of brotherhood,
which also involved heirship. But he soon abandoned this
Une, and expressly recognized the validity and sacredness,
within Islam, of the old rights of family and inheritance
(sur. viii. 76). Thus he refrained from carrying out to
its full logical consequence the theoretical principle of
equalization, but on practical grounds permitted the old
order of society to continue. At a subsequent period, he
even conceded to relationship and the ties of blood far
larger rights than were compatible with Islam, and thus
himself laid the foundations of the violent quarrel which
rent the community, more particularly in the time of the
Omayyads. Similarly it might be said that communism
was originally involved in the principles of Islam ; but it
is characteristic that from the first the alms were less em-
ployed for the equalization of society, than for strengthening
the hands of the ruling power. It frequently happens that
a religious revolution finds expression also in the region of
social polity ; but it is remarkable to o!)sorvo how Islam
utilized the religious leaven from the first for a positive re-
organization of society, and neutrali/.ed the destructive
tendency which that leaven is wont to show in political
affairs. It did not indeed succeed in totally destroying the
radical tendency, as. the history of the caliphate shows.
But, on the whole, the equality before God which Islam
teaches interfered hardly at all with the subordination of
men to their human leaders ; both were demanded by
religion, both were taken sincerely, and each was found,
in practice, rcconcilablo with the other.
That this new .'<nd drastic principle, thrown into the
chaos of existing relations, must have exercised a mighty
power both of attraction and repulsion is obvious. Mora
than one naive cxjiression bears w-itncss to the astonish-
ment with which the Arabs regarded the strange spirit
which animated the community of the Moslems — the firm-
ness with which they held together, the absolute and veil-
ing obedience which they gave to their leaders, the reck-
lessness with which they disregarded everything that before
Islam, or outside of it, was looked upon as holy. Some
natures felt themselves attracted by these peculiarities,
especially if on other grounds they felt little difficulty in
severing themselves from their old connexions ; but, on tija
whole, feelings of antipathy prevailed. Even in Medina The
itself this antipathy was widespread. The so-called hj-po- hypo-
crites (monAfikun) were either only half-attached to the"""*"
Prophet or in their inmost hearts unfavourably disposed ;
they were kept from overt action partly by the absence of
a decided opinion, partly by the terrorism which the con-
vinced Moslems exercised. The reproach of hypocrisy
brought against them means chiefly that they did not
manifest a full acceptance of th» new political relations.
They could not reconcile themselves to the position of
having never a word to say in their own town, and of
being compelled to obey the Prophet from Mecca and those
who had come with him. For a time the danger was
imminent that all Medina (the Emigrants of course ex-
cepted) might be infected with hypocrisy, if one may call
it hypocrisy when for a moment nature and blood asserted
themselves against religious discipline and burst its bonds.
The younger portion of the community, however, was on
the whole enthusiastic for Mohammed ; the hypocrites
were for the most part older men, especially heads of
families, who found it difficult to put up with the loss of
political influence which they were suffering. As chief of
their number Ibn Obay is always named, the foremost
man of Medina, whom the Khazraj had thought of crown-
ing as king, before matters were so fundamentally changed
by Islam. Mohammed's attitude towards him and the
hypocrites in general was that of connivance, — thoroughly
appropriate here, where political rather than religious afi'airs
were involved, and the question was one less of principle
than of power.
The founding of the state upon the feeling of fellowship
generated by religion, was without question the Prophet's
greatest achievement : the community of Medina was the
tool, its heroic faith the force, by means of which Islim
attained the results which figure so largely in the history
of the world.^ Jloslem tradition, however, does not stop to
inquire what it was that constituted the inward strength of
Islam, but goes on at once to relate what were its outward
manifestations. Its information on the subject of the period
of Mohammed's sojourn in Medina is given under the title of
"the campaigns (maghizi) of the apostle of God." With
a few of the smaller tribes in the neighbourhood of Medina
(Johaina, Mozaina, Ghifir, Aslam), and with the Khoz;i'a,
Mohammed maintained relations of peace and amity ;
benevolent neutrality gradually grew into alliance, and
finally union with the commonwealth of Medina. But
towards all the rest of Arabia his very principles placed
him in an attitude of war. Ever since Islam from being
a religion had become a kingdom, l-.e was compelled to
vindicate, by means of war against unbelievers, its claims
to supremacy; the conflict of principles had to be settled
by the sword, the sole sovereignty of Allih dcmonstnited
he
' The credit of bi-ing the founder of the Moslem st-ntc
tr.-insferred to 'Om.ir, hut must be left with Mohammed. It wfl'. not
'Omar who created that feeling of oneness which enabled him, for ex-
ample, suddenly to recall a general like Khillid from his career of victory
without eliciting a murmur. Tlie miracle is the "primitive cell " of
Medin.i, not the fact that in course of time success gave it the fi V'-e of
XOBAVMED.]
MOHAMMEDANISM
555
by force to the rebels who showed unwillingness to accept
it. More literally than Christ could Mohammed say of
himself that he was come not to bring peace but a sword.
Islam was a standing declaration of war against idolaters.
Th« holy The nearest object against which to direct the holy war
w«r. (jihid) was presented by the Meccans. Against them first
did Mohammed bring into operation tb-n new principle, that
it is fcuth and not blood that separates and imites. Ac-
cording to Arab notions it was a kind of high treason on
his part to leave his native town in order to join a foreign
society ; on the part of the people of Medina it was an
act of hostility to Mecca to receive him among them.
The Meccans would have been fully justified on their side
in taking arms against the Moslems, but they refrained,
being too much at their ease, and shrinking besides from
fratricidal war. It was the Moslems who took the initia-
tive ; aggressiveness was in their blood. Mohammed
began with utilizing the favourable position of Medina, on
a mountain spur near the great highway from Yemen to
Syria, to intercept the Meccan caravans. Originally he
sent forth only the Emigrants to take part in the expedi-
tions, as the people of Medina had pledged themselves to
defend him only in the event of his being attacked ; soon,
however, they also joined him. What first induced them
to do so was the prospect of booty; afterwards it was im-
possible to separate themselves, so great was the fusion of
elements which had been quietly going on within the
crucible of Isl^m.
The first plunder was taken in the month Eajab, A.H. 2
(Autumn 623), in which circumstance was at once seen the
advantage arising from the change of conscience brought
about by the new religion; for in Rajab feuds and plun-
dering raids were held to be unlawful. Relying upon the
sacredness of this month a caravan of Koraish was return-
ing from tiii laden with leather, wine, and raisins. But
this did not prevent Mohammed from sending out a band
of Emigrants to surprise the caravan at Nakhla, between
TAif and Mecca ; his orders to this effect were given in a
document which was not to be unsealed untU two days
after the departure of the expedition. The plan was carried
out, and the surprise was all the more successful, because
the robbers gave themselves the outward semblance of
pilgrims ; one Meccan was killed in the struggle. But
the perfidy -n-ith which in this instance Mohammed's ad-
vanced religious views enabled him to utilize for his own
advantage the pious custom of the heathen roused in
Medina itself such a storm of disapproval, that he found
himself compelled to disavow his own tools. In Moham-
medan tradition, the contents of the unambiguous document
in which he ordered the surprise are usually falsified.
Battle of The Koraish still remained quiet ; another outrage had
Bedr. yet to come. In Ramadan A.H. 2 (December 623), the
return of their great Syrian caravan was expected, and
Mohammed resolved to Ue in wait for it at Bedr, a favour-
ite watering-place and camping -ground, northward from
Medina. For this purpose he set out thither in person
along wifh 308 men ; but the leader of the caravan, the
Omayyad Abii Sofyin, got word of the plan and sent a
messenger to Mecca with a request for speedy help. Con-
cern about their money and goods at last drove the Koraish
to arms ; a very short interval found them, 900 strong, on
the road to Bedr. By the way they received intelligence
that the caravan had made a circuit to the west of Bedr,
and was already in safety. Nevertheless they resolved, at
the instance of the Makhzumit Abii Jahl, for the sake of
their honour, to continue their march. When the Moslems
first got touch of them at Bedr, they took them for the
caravan ; their surprise on discovering the truth may be
imagined. But, kept firm by the courage of their leader,
they resolved to face the superior numbers of the enemy.
On the morning of Friday, the 17th of Ramadan, the
encounter took place. A number of duels were fought in
the front, which were mostly decided in favour of the
Moslems. The Meccans at last gave up the fight, strictly
speaking for no other cause than that they did not see any
reason for carrying it on. They were reluctant to shed
the blood of their kinsmen ; they were awestruck in pre-
sence of the gloomy determination of their' adversaries,
who did know what they were fighting for, and were
absolutely reckless of consequences. After a number of
the noblest and oldest of the Koraish, including at last
Abii Jahl, had fallen, those who remained took to flight.
The number of the dead is said to have been as great as
that of the prisoners. Two of the latter, whom he per-
sonally hated, Mohammed caused to be put to death
X)kba b. Abl Mo'ait and al-Nadr b. al-H4rith. A\"hen
the last named had perceived, from the Prophet's malignant
glance, the danger in which he stood, he implored an old
friend of his among the Moslems for his intercession. This
request being refused, al-Nadr said : " Had the Koraish
taken thee prisoner, thou hadst not been put to death as
long as I had lived ;" to which the apologetic reply was :
" I do not doubt it, but I am differently placed from thee,
for Islam has made an end of the old relations." To the
remaining prisoners life was spared on payment by their
kinsmen of a heavy ransom ; but Mohammed is said to
have afterwards reproached himself for having allowed
considerations of earthly gain to keep him back frcm send
ing them all to hell as they deserved.
The battle of Bedr is not only the most celebrated of Effect
battles in the memory of Moslems; it was really also ofoff"
great historical importance. It helped immensely to ''*"''■
strengthen Mohammed's position. Thenceforward opei:
opposition to him in Medina was impossible ; families
which had hitherto withdrawn themselves from his influ-
ence were so thoroughly cowed by some atrocious murders
carried out in obedience to his orders, that they went over
to Islam. He was now in a position to proceed to brcilc
up the autonomy of the Jews. In the first instance he
addressed himself to the weak Banii Kainoki, demanding'
their acceptance of Islam; on their refusal, he took the
earliest opportunity that offered itself to declare war against
them. After a short siege they were compelled to surren-
der; and they might congratulate themselves that their old
ally, Ibn Obay, was able to concuss the Prophet into sparing
their lives, and contenting himself with their banishment
frpm Medina. Soon afterwards other blow? were struck,
in the shape of assassinations, by means of which Moham-
med put out of the way several of the Jews whom he hatedl
most, such as KaT) b. al-Ashraf and Ibn Sonaina.' The^
state of fear to which the rest were reduced may readily
be imagined ; Hiey came to the Prophet and begged him
to be propitioxis. If in other days their dislike had found
somewhat public expression in all sorts of witticisms and
scornful sayings, they were now at least modest and quiet,
and kept their hatred to themselves.
The Meccans also were very deeply impressed by the
defeat inflicted on them by the Moslems. They saw clearly
that the blow must be avenged, and they took comprehen-
sive measures for their campaign. After a year's delay,-
their preparations being now complete, and their allies
* The murderer of Ibn Sonaina was Mohayyisa b. Mas'ud, of whose]
elder brother, Howaisa, he had been a sworn ally. Howaisa struck the'
murderer in consequence, and reproached him with his treacherous
ingratitude, saying that much of the fat in his body had come fromi
the estate of the Jew. Mohayyisa's reply was : " If he who bade mo
kill him were also to bid me kill thee, I should obey." The brother,
amazed, asked him if he was serious, and when the other assured him
that he was, Howaisa exclaimed : " By God, a religion which brings it
to this is a stupendous one, " and fortliwith became a "opvprt. The
storj* ( f'ttkidi, p. 981 is too characteristic to be j>.'issed OTtl.
656
MOHAMMEDANISM
[SIOnAMMED'
(AiabisL) assembled, they set out under the command of
Abii Sofyin, and without any check reached Medina, where
they pitched their camp to the north-east of the city, in
the green corn-fielda by Mount Ohod. In Medina the
ciders were for awaiting the attack on tie town and de-
fending themselves within it, but the young men hurried
the Prophet into the determination to meet the enemy
without the gates ; this resolution once come to he per-
, severed in, even after those who had urged him to it had
"JBit-I^ of changed their minds. On the morning of Saturday, the
■Oho'l. 7th of Shawwal, a.h. 3 (Jan. Feb. 625), the armies met.
At first the battle seemed to be going once more in favour
of the Moslems ; one after another the standard-bearers
and champions of the enemy fell, the whole host \vavered,
and even the camp was gained. But here their lust for
plunder did them au evil turn. Mohammed had covered
his left flank against the Meccan horsemen by a number
of bowmen, whom he liad ordered on no account to leave
their post. But as soon as they saw that the enemy's
camp was taken, they threw off aU discipline,, and
determined to have their share of what was going. *t
thus became possible for the Meccan cavalry to fall upon
the iloslem rear, and snatch back the victory that had
already been won. In the confusion which now ensued
Mohammed himself was wounded in the face, and for some
time lay for dead on the ground. Among the slain was
found his uncle, Hamza b. "Abdalmottalib, "the Hon of
God ; " his liver was cut out and carried to Abd SofyAn's
wife. Hind bint "Otba, whose father had been killed by
Hamza at Bedr. But the Meocans did not know how to
follow up theii' triumph. Instead of at once attacking
Medina — where, to be sure, a second struggle with Ibn
Obay, who with his following had not taken part in the
battle at Ohod, would have been necessary — they con-
tented themselves with the honour of their victory, and
took the road home, after havidg summoned the Moslems
to a repetition in the following year of the duel at Bodr.
Mohammed even pursued them for a short distance on the
following day (as far as to Hamri al-Asad), of course only
for the sake of appearances, that the Arabs might not
suppose him to have been daunted by his defeat.
■Ban* Nothing came of the proposed meeting at Bedr, the
*"' 11 J ^^^'^'^^°^ failing to put in an appearance. The principal
■V" ^ ■ event of a.h. 4 was the expul.sion of the Banii Nadir,
the most distinguished and powerful Jewish family in
^Medina (Summer 625). Mohammed, under some pretext,
suddenly broke with them and ordered their departure
wi'Mn ten days, on pain of death. Kelying upon the
support of Ibn Obay, they resolved to resist, and sus-
tained a siege within their walls ; but the ally they had
counted on proved a broken reed,' and they were soon
compelled to surrender. They were permitted to with-
draw, taking along with them all their movable property
except their arms. With music and roll of drum, the
women in gala dress, they marched through the streets of
Medina, on their way to Khaibar, where thoy had pro-
perty. Their land the Prophet appropriated to himself
(sur. lix. 7) ; the income derived from it could bo e:n-
|)!oyed to meet the numerous claims that were made upon
him. He seems also to have handed over some of it to
the Emigrants, who until then had acquired no property
in land in Medina.
Meanwhile, the Banu Nadir were not idle in Khaibar,
but left no stone unturned to annihilate their mortal
f nemy. Thoy succeeded in bringing about au alliance of
the Koraish and the great Bedouin tribes of Solaim and
Ghatafdn, for the suppression of lilam. In the month
' Tlie sympathy ahown by many scholars for Ibn 0'<ay, whose we.ik.
ness degenerated into failUlessnesa, is tinj>:stif'.cd.
Dhii 'l-ka'da, a.h. 5 (March 627), the three armies aft-
out, 10,000 stirong, under the command of Abii Sofyiin.
Mohammed received word of this through the Khozi'a,
who secrptly played into his hands, and on this occasioa
he resolved, not as formerly to offer battle on the open
field, but to make preparation for a siege. For the most
part the houses of the town were built so close to one
another as to make a continuous wall ; at the north-west
corner only was there a wide open space, through which an
enemy coiild easily effect an entrance. Here Mohammed,
■with the advice and direction of the Persian freedman
Salman, drew a ditch, behind which he entrenched him-
self with the Moslems, the lull of Sal'- protecting their
rear. This fosse, which has become famous, and has even
given its name to the entire campaign (the War of the ^ar rf
Fosse), fully served its purpose. The enemy with their '-"'
cavaliy perseveringly directed their attack on this spot, '"^^
but were constantly repelled by the vigilant and courageous
defence of the fosse. They at last gave up all hope of
reaching their end in this way, unless a simultaneous
attack were to su^'ceed in another quarter. To assist
them in this, they endeavoured to stir up the Koraiza, the
last autonomous family of Jews still remaining in Medina,
having their settlements in the south-east of the town.
The Nadirite Hoyay b. Aklitab, the most zealous promoter
of the alliance against Mohammed, undertook charge of
the negotiations, and succeeded at last in persuading their
prince, Ka'b b. Asad, to break his pact of neuti>.lity with
the Moslems. But nothing came of it. The Jews doubted
the perseverance of the Koi-aish and their allies — they had
their fears lest, if the struggle proved a protracted one, the
besiegers might withdraw and leave them to their fate.
They accordingly demanded hostages in security against
such an event, being otherwise determined not to break
up all hope of reconciliation with Mohammed by entering
the contest. This attitude, in turn, aroused suspicion on
the part of the besiegers, whom it was not difficult to con-
vince that the Jews were demanding hostages of them for
the purpose of handing them over to Moharumed, and so
making their peace with him. All this crippled their actlvi-
ties still more than did the failure of their o-n-n attacks upon
the fosse. The season also was against them ; the weather
was windy, the nights extremely cold, and, worst of all, the
fields yielded nothing. From this cause the chief sufferers
were the Bedouins, who had brought no forage for their
camels and horses. Mohammed, who appears to have been
kept well informed of their mood, judged it expedient to
open negotiations with them. These were soon broken off
indeed, but the mere fact that the Ghatafdn had ever
entered upon them was enough to create mutual suspicion
amongst the allies. One stormy night the Meccana
suddenly raised the siege, after it had lasted fourteen
days, and returned home ; they were followed by the
Ghataf.^n and Solaim. It was with no small joy that the
Moslems on the following morning discovered the de-
parture of the enemy ; it would have been impossible for
them to have held out much longer, exliausted as they
were, not less by cold and hunger, than by the fatigues of
constantly mounting guard. As soon as Mohammed had
given them permission to leave the camp beside the hill
of Sal', they dispersed with the greatest alacrity to their
homes.
Mohammed, however, did not allow them much time to i^-:it
recruit. Hardly had they reached their abodes, when ho »? ""
again called them to arms against the treacherous Koraiza. ':'^'""J»'
The unlucky Jews had been given over to the sword by
the withdrawal of the allies ; a siege of fourteen days
compelled them to surrender unconditionally. The men
' Now the citadel, it would seem.
JfOHAMJU:!).]
H 0 H A: M M E D A N I S M
55?
■nere^driven in cbains to the house of Osima b. Zaid,
whence on the follnwing morning Mohammed caused them
to be brought one by one to the market-place of Medina,
Olid there executed. This continued till late in the even-
ing. They were six or seven hundred in number, and
among them was the Nadirite Hoyay b. Akhtab, the
author of the War of the Fosse, Trho had left the Meccans
to join his fortimes with those of the Korai7a. By
accepting Islam these men could have saved their Uvea,
^ut they preferred deatL No more magnificent martyrdom
.lis known to history. The women end children were sold
(into slavery ; one young woman only, EanAna, suffered the
I j)enalty of death for having broken the head of a Moslem
hvith a millstone during the siege. With joyous heart and
.'smiling face she went to meet her death, never forgotten
I, by 'Aisha, with whom she was when her name was called.
The Prophet selected for himself the fair Raihdna, and
married her, aftor having caused her to become a convert
to Islam.
The War of the Fosse was the last attack made by the
Koraish upon Medina ; Mohammed now began to take the
offensive towards Mecca. This he at first set about with
extreme diplomacy, utilizing the festival, and the truce of
God subsistins; at the time of the festival, for the purpose
of paying a visit to his native town. Although unsuccess-
ful in winning to his side the neighbouring tribes of
Bedouins, it was nevertheless with a considerable following
(1500 men) that in Dhii '1-lca'da A-H. 6 (March 628),i he set
out on his journey. In a dream he had had the key of
the Ka'ba delivered to him ; on the strength of this his
followers believed fiiinly in the success of the expedition.
But the Koraish were determined that the pretext of pil-
grimage should not avail their adversary ; they summoned
their allies and formed a camp to the north of their tovt-n
for the purpose of preventing the entrance of the Moslems.
Mohammed was forced to halt at Hodaibiya on the borders
of the sacred territory, and it was in vain that by fair
speeches he sought to obtain permission to make the
circuit of the Ka'ba. He felt himself too weak to force
his way, and accordingly preferred ' > treat. While the
envoys were passing to and fro, there suddenly arose an
alarm in the Moslem- camp ; they apprehended a sudden
act of treachery on the part of the Meccans. It was on
this occasion that the famous Homage under the Tree took
place, when Mohammed pledged his followers by striking
hands that they would stand by him and go to death for
his sake. Some of the Koraish agents witnessed the scene,
and were immensely impressed by it ; such an enthusiastic
obedience as Mohammed received, such- an ascendency over
the minds of men as he exercised, they had never before
conceived to be possible, and on their return they urged
their people in the strongest way not to permit matters to
come to extremities. The Koraish accordingly judged it
best to offer a bargain with Mohammed, the terms being
that for this year he was to withdraw, so that the Arabs
might not say that he had forced an entrance, but that on
the following year he yras to return and be permitted to
remain' three days -n-ithin the sacred territory for the
purpose of sacrifice. After some discussion Mohammed
accepted this proposal, although zealous Moslems detected
a discreditable shortcoming in matters of faith, in so far as
it involved turning back within sight of the Ka'ba without
being allowed to accomplish the sacred circuit. W hen the
agreement was to be committed to writing, Mohammed
dictated the words : " In the name of Allih, the mercii'ul
E«hraAn";^ but the Meccan plenipotentiary, Sohail b.
'Amr, declared that be knew nothing about Rahmdn, and
' Noldeke, Tabari, p. 803, note 1 ; rahidi, p. 18.
^ Kalituuii is a name of God which Mohamin&d had token fromihe
Ji,"ffs and Bscd with fpecia! preference.
insisted upon the custowaiy formula — " In thy nan/e,'95B4-
hormna!" The Moslems murmured, but Mohammed
yielded. He then went on to dictate : " This is the treaty
of peace between the apostle of God." . . . Sohail anew-
protested ; to acknowledge Mohammed as the apostle of
God, would be to declare himself his follower ; the^dcr
signation ought to be simply Mohammed b. 'Abdallih. The
Moslems murmured louder than before, and refused to
consent to the change. The heads of the two tribes of
Medina, Osaid b. Hodair and Sa'd b. 'Obida, held the
hand of the scribe and declared that "Mohammed tho
apostle of God " must be written, or the sword must de-
cide. The Meccan representatives whispered to one
another words of amazement at tho spirit displayed by
these men. But Mohammed made a sign to the zealots
to hold their peace, and again gave way (sur. xviL 110).
The writing which now took shape ran as follows : —
" In thy name, 0 God I This is the treaty of peace concludei', The
by Mohammed b. 'Abdallih and Sohail b. 'Amr. They have agreed treaty,
to allow their arms to rest for ten years. During this time eacli
party shall be secure, aiid neither shall injure the other ; no secret
damage shall be inflicted, but uprightness and honour prevail be-
twkt us. Whosoever wishes to enter into treaty and covenant with
Mohammed can do so, and whosoever wishes to enter into treaty
and covenant with the Koraish can do so. But if a Koraishite
comes without permission of his guardian (Wall) to Mohainmed, he
shall be delivered up ; but if, on the other hand, one of Mohammed's
people comes to the Koraish he shall not be delivered up. This
year Mohaiamcd with his companions must withdraw from us,^ but
next year he may come amongst us and remain for three days,
yet without other weapons than those of a traveller, the swords
remaining in their sheaths."
The first result of the treaty was that the Khozi'a de-
clared for alliance with Mohanuned ; while, on the other
hand, the Bekr b. KlinAna joined themselves to the
Koraish.
To compensate his followers for the apparent resultless- WarwHU
ness of this expedition, Mohammed immediately after K''^'""'-
their retiun led them out against the rich Jews of Khaibar
(northwards from Medina), whither the Banti Nadir had
migrated, and from which place they hi^l unceasingly
stin-ed up opposition against the Prophet. Hitherto ho
had contented himself with putting out of tte way, by
means of assassination, some of their leading men who
seemed to him to be particularly dangerous, such as Abii
Rifi' and Yosair b. Rizim,* but now he resorted to whole-
sale measiu'es. In Moharram, a.h. 7 (May 628), he mado
his appearance before Khaibar with a powerful army ; in
the plunder only those who had taken part in the. expedi-
tion of Hodaibiya were to share, but many others besides
accompanied them. The Jews, although aware of the
hostility of Mohammed's intentions, were nevertheless
taken completely by surprise when oneinoming they saw
him and his troops encamp before their strongholds. One
of their leaders had given them the excellent advice not
to shut themselves up by families in their quarters, but to
construct a common camp in the fields, otherwise they
were likely to share the fate of their coreligionists in
Medina. But they replied that their strongholds were of
a different sort, perched on impregnable summits, and
they remained shut up within 'hem. They had neither
discipline nor order, courage nor devotion. As they were
wanting in community of feeling, so also were they lacking
in leaders. Their best man, Salim b. Mishkdm, lay on a
sick-bed ; his place was by no means supplied bj' Kinina
b. b. Abl 'l-Holfa<t When they suddenly became aware
that they hsid been completely abandoned by their Arab
allies, the Ghataf An, their heart utterly failed them. When
besieged in any of their citadels, they hardly ever waited
5 The " us " is remarkable, and sounds as if the treaty hail Wen
dictated by the Meccans.
KJakiilu pp. .170, 239.
'658
MOHAMMEDANISM
[MOHAilMED.
to be stormed, but after one or two sorties evacuated it
and withdrew to anotlier, where the same story was re-
peated. Thus citadel after citadel fell into the hands of
Ruin of the Moslems ; treachery, which had something to do with
thB Jews, the surrender, was well-nigh superfluous. From Al-NatAt
the Jews were driven to Al-Shikk, and at last nothing was
k :t to them but Al-Katlba (with Al-WatOj and SolAlim).!
There they remained shut up and filled with fear, without
even risking, as formerly, single combats and skirmishes
before their citadels. After some time they asked for
peace, and obtained it on the footing that they retained
their lives, wives and children, and one garment each, but
gave up all their property, the penalty of concealing any-
thing being death. KinAna b. b. Abl '1-Hokaik was cruelly
tortured, and at last put to death because he had buried
the renowned jewels of his family ; thus at the same-time
his handsome wife Safiya bint Hoyay was left free for
Mohammed.
His marriage with "the daughter of the king" wound
np the prosperous campaign. gaffya felt no repulsion
towards the man who had caused the death of her father
Hoyay, and of her husband Kindna ; she gi-acef ully accom-
modated herself to the situation. More worthy was the
demeanour of another Jewess, Zainab, who made the
attempt to poison the executioner of her people, and
atoned for this offence by her deatL The attempt was
unsuccessful, but Mohammed believed that even in his
last illness he could trace the effects of the poisoru ^
Simultaneously with Khaibar, Fadak also fell into his
hands, and shortly afterwards Wadi '1-KorA, where also
there were settlements of Jews. The plunder was very
considerable. So far as it consisted of movables, it was
gathered together into a heap, and put up to auction ; the
proceeds were then divided. Mohammed insisted very
strictly that no one should be permitted to plunder for
his own hand. The property in land, palm plantations,
vegetable gardens, were allowed for the time being to
remain at a rent in the hands of the Jews ; half of the
produce had to be paid to the new owners. The lion's
share of the spoil fell to the lot of God, i.e. of the Prophet
— a fifth of the movables, of the real estate a larger pro-
portion. He con.sequently had at his command consider-
able material resources, and he well knew how to employ
them, not only for the enriclunent of his family, but also
for gaining over to his side such individuals as were
more accessible to payment than to principles.
The peace of Hodaibiya, with the subsequent conquest
of Khaibar, closes the first period of Mohammed's life at
Medina ; strictly speaking, indeed, it merely confirmed the
status which in point of fact the War of the Fosse had
already given him. If at first it seemed as if Mohammed
had shamefully given way, it soon became apparent, never-
theless, that the advantage lay with him. "No victory of
Islam," Abiibekr was wont to say, " has more importance
than the treaty of Hodaibiya ; men are always for hurry-
ing things on, but God lets them ripen." "Previously
thfere had subsisted a wall of partition between the
Moslems and the rest of men ; they never spoke to each
other ; wherever they met, they began to fight. Sub-
sequently hostility died down ; security and mutual con-
Rapid fidence took its place. Every man of even moderate intcl-
spread of li-Tence who heard of Islam joined it ; in the twenty-two
months during which the truce subsisted, the number of
conversions was gieatcr than throughout the whole of the
previous period ; the faith diffused itself in all directions
among the Arabs."
As a religion Islam did not attract the Arabs ; they had
' Such were the names of the three separate quarters of Khaibar,
CAch ODQ made up of a complex of hou^s oud citadels.
no inclination to pray, reaa the Koran, and cive alms.
Of this they had given sufficient evidence by their per-
ennial feuds with Mohammed, and by the murder of
divers of his missionaries who were sent to teach them
the faith.2 We can hardly believe that a new spirit now
suddenly possessed them. Their change of attitude was
merely due to the imposing cfi"ect of the rising might of
Islam. They began to respecjt the Moslems, who, in spite
of their small numbers, could defy a whole world, because
they were of one mind, and did not ask what the world
thought. They saw that, in the great conflict between
Mecca and Medina, in which as actors or as spectators
they had all participated, the victory inclined more and
more to the side of Medina, that force could accomplish
nothing against faith. The prestige of Mecca was shaken
by the War of the Fosse, and was not restored by the treaty
of Hodaibiya, in which the Koraish waved Mohammed off
with the open hand, and at the same time permitted him
to return next year. Islam had " stretched out its neck "
— had consolidated itself into indestructible existence —
it now fought for victory. There was, moreover, another
argument in favour of the new religion, to which the Arabs
were very sensible — the rich booty, to wit, which the
Moslems acquired by their continusJ forays. There is no
question that the material success of Islam was the chief
force that attracted new adherents.
The treaty of Hodaibiya gave a breathing space to the Results
two combatants, and of this the prophet reaped the whole "f the
advantage The truce, which lasted for almost two years, '"i"
brought to the Meccans an almost unbroken series of jfjcca.
humiliations and losses. Contrary to all expectation, the
provision made in their favour, by which Mohammed
bound himself to send back such of their sons as deserted
to him before their majority, turned to their hurt, so that
they had to ask Mohammed to have it changed.' Still
more serious for them was the desertion of three eminent
men, KhAlid b. al-WaUd, 'Amr b. al-'As, and 'Othmdn b.
Talha, whom the Prophet received with open arms. Next
year they looked on with shame and concealed indignation
when the Prophet, availing himself of his stipulated right,
entered the city with 2000 men, and performed the sacred
ceremonies ("Omrat al-KadA, March 629). Still they were
afraid to break with him again, and did not even venture to
rid themselves of his spies, the KhozA'a, who lived in their
midst. " When they put one foot forward they draw the
other back ; they are convinced that Mohammed will
win" — such was the impression the Koraish made on the
Bedouins, who have a very keen instinct in matters of
this sort. They had lost confidence in themselves ; they
knew that the fight was not fought out, but they dared
not seek to bring it to a decision.
Against their vnU. the decision came. The Bani'i Bekr
fell upon Mohammed's friends, the KhozA'a, and were
supported by some of their Koraishite allies. The KhozA-
1
' See Vakidi, pp. 153-157 (Bir Ma'iina and al-Raji'), and the general
view of these feuds, ibid. p. 29 sqq.
* Abii Basir had fled to Mohammed to Medina ; the Meccans de-
manded his surrender. He was given u;i, in spite of his passionate
j*emonstrances, to the two messengcre sent to fetch him. But on the
road he fell on one of them and slew him with his own sword ; the
other hastened bnclt to Medina in horror. AbA Basir foUovcd,
thinking Mohammed had now done enough to satisfy the Meccans.
Only, however, when the messenger refused the charge of so dangerons
a prisoner, did Mohammed permit the latter to go off where he pleased,
refusing to allow him to stay with the Moslems. Accordingly Abd
Basir made for the coast-road of the Syrian caravans, and became the
leader of other Moslem fogitives from Mecca, who quickly gathered
round him. They intercepted all caravans, divided the prey, and
slew the men. Abii Basir's robberies at length induced the Meccans
to ask Mohammed by letter to allow him to join his community, and
so put an end to the miichici. — Kakidi, p. 261 ; 7,bn lliihim, p
757 sqq.
MOHAMMED.]
M O. H A M M E D A N I S.M
559
ilea complained to the Jfrophet, who eagerly seized the
pretext for war. In vain did the Mecoans send Abii
Sofydn to Medina to renew the truce; they could not
move the Prophet from his purpose. In Ramadan, a.h. 8
Tb» (January 630), he. moved against Mecca with an army of
*" " 10,000 men. ' With the Emigrants and the Defenders were
'^'^'"^ ■ mustered the Aslam, GhSir, Mozaina, Johaina, and
Ashja' ; the Solaim and the Khozi'a joined them on the
way. The Bedouins were drawn by the hope of booty ;
the Fazirite 'Oyaina was sorely vexed that he had left his
Ghatafin at home, not knowing what v/aa in view, for
Mohammed at first kept the aim of his expedition a secret.
Some of the Meccan nobles must, however, have known
it ; Makhrama b. Naufal, for example, and the Prophet's
uncle, 'Abbds, did not await the capture of their city, but
deserted to the enemy while he was still distant. Abi
Sofydn, in particular, must have been in the secret; it
appears that at Medina he received the promise that the
holy city should be spared if it yielded pacifically, and
that he pledged himself to do his best to play into the
hands of the Prophet.* But before the populace it was
necessary to keep up the appearance of a sudden surprise,
an inevitable submission to an unforeseen display of force.
The same comedy was repeated afterwards at fiii ; the
headmen treated with the Prophet without consulting the
Thakafites, and then contrived that the result of their
policy should appear to be forced by the course of events.
The Moslems were on the border of the holy land before
the Meccans suspected their approach ; then suddenly one
night 10,000 fires were seen rising to heaven to the north-
west of the holy city. In well-feigned surprise Abil SofyAn
Conquest hastened to the hostile camp ; he returned with the news
or Mecca, jij^j Q^^ Moslems were at the gates, that an improvised
resistance could effect nothing against their force ; the only
wise course was a surrender — Mohammed had promised
security to those who remained in their houses or threw
away their weapons. The terrified Meccans had hardly
any other course open to them than to follow this advice.
And now the Moslems entered the city from several sides
at once, meeting only at one point with an easily quelled
resistance. Mohammed insisted that there should be no
violence ; he pledged the captains to avoid all bloodshed.
Ten persons only were put to tho ban, and of these onfl
half were subsequently pardoned. He took all pains tO'
preserve the sanctity of Mecca unimpaired, confirriied the
rights and privileges therewith connected, and made it
plain that the old cultus should not be less flourishing
under Islam. The ceremonies were retained, save only
that he abolished all idols, both the domestic gods found
in every house'and the images in and round the Ka'ba.
But every sanctuary outside of Mecca was destroyed,
except siich as had a part in the celebration of the Feast,
and so stood in connexion with the Ka'ba itself. Thus
the Meccan worship gained a new and unique importance.
Mohammed's reform did for Mecca what Josiadi's did for
J«rusalem.2
The last step towards that identification of the Ka'ba
with Islam, which made it the religious centre of the
Moslem world, was not taken tUl the following year, when
the famous Renunciation (Bar4'a) of sur. ix. forbade the
heathen to share in the Feast, which was henceforth to be
a strictly Moslem ordinance, and at the same time abro-
gated the peace of the holy months. A year later (Dhii 1-
Hijja, A.H. 10, March 632) he himself celebrated the Feast
for the first time in the orthodox fashion, introducing
' certain modifications on the traditional practice and
* The tradition indeed is silent, but Muir (iv. 120) is jostif
drawing thij inference from the course of events.
* Ssouck-Hni^onje, Het Mekkaansche Feat, Leyden, 1880.
reducing certain varieties of use to uniform rule. In all
this he professed to re-establish the true ancient use,
purged of heretical deviations from the example of-
Abraham. At the same time he remodelled the Calendar,'
forbidding the occasional interpolation of a month as an
arbitrary and human invention, and establishing the true
lunar year of twelve lunations.
We return to the capture of Mecca. The submission of War
the Koraish was followed by that of their nomad brethren ™'"'
and allies. But the neighbouring Hawilzin, to whom *^," .^"*
belonged also the Thaljafite inhabitants of TAif, assembled ^'^"''
lor battle with the Moslems. They camped in Autis
between Taif and Mecca. Mohammed advanced against
them, and battle was joined in the vaUey of Honain. The
Moslems were broken by the first charge of the foe; for a
moment the Prophet himself was in danger, till the Khazraj
rallied round him, checked the onset of the Hawixin, and
at length turned them to flight. A vast booty rewarded
the victors ; for the Hawazin had brought all their herds
and non-combatants with them and placed them in the
rear, that they might feel what they were fighting for.'
Mohammed caused the prey to be conveyed to thb glen of
Ji'rdna, outside the north-west border of the Haram, a little
way off the great valley that descends from T^if ; he him-
self pressed on to T^if itself. Here, however, he failed in
his object ; in a dream he saw a cock peck a hole in a
bowl of cream that was set before him, so that the con-
tents ran out. After fourteen days he gave up the siege
and marched to Ji'rAna to deal with the booty. He had
deferred this task in the hope that the HawAzin would be
tempted to embrace Islam in order to recover their
families and cattle. But as they still sent no ambassadors,
he had- to yield to the pressure of the Bedouins and divide
the spoil. When it was 'too late, the messengers of the
Hawdzin appeared to announce their conversion ; they
had now to give up their herds, and content themselves
that their wives and children were restored to them,
through the mediation of the Prophet with their new
masters. The Bedouins received compensation for what
they gave up ; the Emigrants and Defenders gave up their
captives freely. Altogether the men of Medina fared
worst in the distribution of booty, though they had borne
the brunt of the conflict ; those who fared best were the
nobles of Mecca, who had no share in the fight, but whom
Mohammed desired to conciliate by gifts (sur. ix. 60).
The fall of Mecca reacted powerfully on the future Aggmn-
development of Islam. Again the saying came true : direnieut
victa victoret cep«< /^ the victory of the Moslems over the ?f "'? .
Koraish shaped itself into a domination of the Koraish '
over the Moslems. For this the Prophet himself was. to
blame. In making Mecca the Jerusalem of Islam, he was
ostensibly moved, by religious motives ; but in reality
Mohammed's religion had nothing to do vrith the
heathenish usages at the Ka'ba and the Great Feast. To
represent Abraham as the founder of the ritual was merely
a pious fraud. What Mohammed actually sought, was to
recommend Islam to Arabic prejudices by incorporating
this fragment of heathenism, and at the same time he was
influenced by his local patriotism. Henceforth these
local feelings became quite the mainspring of his conduct ;
his attitude to the Koraish was determined entirely by
the spirit of clannishness. Hence the extraordinary value
he set on the conciUation of their chiefs ; one gains the
impression that he cared more for this than for the con-
version of all the rest of the world. He left to them all
that they already had ; he gave them in addition whatever
they asked, if only they would be his good friends. Abii
Sofydn was a great man already, but Mohammed hastened
* Among them were relatives of the Prophet's foster-mother, Haliffla.
jGO
M O II A :\I :»I E D A. K ISM
[mohammedJ
to raise his power by giTin;;; I. Pin rule over a t/roaJ tract
southward from Mecca. He used every means to make
th':ir conversion easy to the Koraish, and to convince them
that they were losing little and gaining much. They liad
the sense to understand this' and act accordingly ; they
were soon the best of Moslems, and that for the best
practical reasons.
The men of Medina, as wa-s natural, felt thetnselves
slighted in a special degree by this petting of the Koraish.
They had done all and sacrificed all for the Prophet; were
others now to reap the fruit of their labours 1 Had thoy
by years of struggle made Moliammed Lord '«f Mecca,
only that they might surrender in favour of Mecca the
place they had hitherto held t Did he indeed esteem kin-
ship so much more than tried service to the Faith I The
Defenders had good ground for discontent, but Mohammed
appeased them easily enough. He rcmiuded them of
their fellowship together in the great days of the past, of
all that he had done for them, and they for him ; he
Ijromised that their town should still be his residence,
and so the political capital of Islam (Madinat al-IslAm).
Then all the men wept till their beards were wet, and
said : " O apostle of God, we are content with our share
and lot ! "
Yna The Defenders murmured at the preference shown to
Khdri- the Koraish, because they desired preference for them-
jit'js. selves. But already there were movements of an opposi-
tion from principle which deemed it a falling away from
Islam to give ;iny heed to kinship instead of to faith. It
is related that the beginnings of the Khilrijites (Dis.senters)
go back to the distribution of booty in W. Ji'rAna.'
Certain it is that a worldly bias, which had indeed been
introduced into I.slam long before, then first became
visible to every eye. Certain it is that Mohammed then
sowed the seeds of the deep dissensions that rent his
following after his death — of the struggle between religious
democracy, such as Islam demanded, and the national
aristocracy, which alone was really fit to hold rule in
Arabia. It was Mohammed who placed the helm in the
hands of the Koraish and opened the way to sovereignty
for Abu Sofy'in and his house, the Omayyads. If the
KhArijite Dhu '1-khowaisira spoke out against the Prophet
himself at JiVana, the feeling that moved him was cjuite
sound.
The last years of the Prophet were like the ingathering
of a harvest laboriously reaped. The conquest of Mecca,
so great was the impression it produced, w"as called " fJie
Conquest," as if it contained in itself all otherii. From
Conver- every side, in the next two year.% the sheikhs streamed to
eiui of Medina to open negotiations for the acceptance of Islam
A'-aWfk jjy tjjgij. tribes ; if they did not come spontaneously,
Mohammed sent to them. A change of heart on the part
of the Arabs had no more share in these than in former
conversions. It cost them no struggle to cast away their
idols ; the images and the .sanctuaries i'ell quietly enough.
Heathenism was a dead thing ; superstitions could be
transplanted into Islam. The unique sovereignty of
AU.'lh Avas clearly evidenced in the fact that no might
could withstand his. It is safe to afiirra that the acces-
sions to Islam were due to political more than religious
impulses, and meant adherence to the stale of Medina
rather than to monotheism. The power to which that
city had grown, acted as a force of attraction upon the
Arabs ; and their subjection was not the mere efi'ect of
fear, but expressed also that sense of the necessity for
peace and order, which had led to the foimding of states
in the two previous centuries. Thus it becomes intelligible
that from every side, by a sort of natural necessity, the
' Vuhidi, p. 377. Ibn Hisl,ani, p. 884.
masses of Arabian society were drawn towards the centre
of attraction at >Iedina, and that the Prophet received
the homage of distant tribes which he could not have
influenced directly. The Christian tribes were not behind
the rest, they were Arabs first and Christiai/S after.
Oidy the Christians of Najran remained true to their
ftdth ; so did the Jews in all parts, and the Magians in
the province of Baljrain." The last named, as idolaters,
ought not in strictness to have been tolerated in the
^Moslem state ; but practical considerations broke through
theory, and the men of system had to accept the incon-
sistency with the best grace they could.
The signs of submission were — (1) the performance of
the five daily prayers, or at le^st the proclamation of the
times' of prayer by the Muedhdhin ; (2) the payment of
the alms-tax ; ^ (3) the acceptance of the Moslem Law,
which was introduced by qualified delegates from Medina.
Otherwise things remained ss they were ; Mohammed was
careful not to meddle with tribal afiairs, and strengthened
the existing aristocracies wherever he could do so. The
change of faith was eftected by treaty ; the populace was
not consulted, and the whole negotiations were directed
by the Elders and Chiefs. For, in fact, purely political
interests were involved.
A single case, about which our information is exception- Tail
ally full, will suffice in illustration. The HawAzin had
joined Mohammed after the battle of Hcmain, and now
preached the dutj' of holy warfare agoinst their kinsmen,
the Thakafites of Taif, who were still heathens. Tliey
made raids on tlif' cattle pastured without the cit_T, and
made captives of those who ventm-ed abroad. The Thal>a-
fites were exposed, alone and helpless, to the advances of
Islam ; they dared not stir a foot beyond their walls. The
heads of the city found the situation untenable, and
resolved to do homage to the Prophet for the sake of
peace. Ten ambas,sadors proceeded to Medina, and nego-
tiations began as to the conditions of the conversion of the
ThaVif. The envoys desired that fornication, usury, and
wine-drinking should be permitted to them ; this Moham-
med refused (sur. xvii. 234 ; ii. 278 ; v. 92) ; and they
consented to yield the point when it was explained that,
indispensable as these three practices might seem, the
other Moslems had learned to give them up. There was
more difficulty about the Rabba or Goddess of T'lif (al-
Lit). The ambassadors begged that, as a concessiou ,to
the foolish multitude, they might retain her for three years.
Wliou they found Mohammed resolute, they came down
successively to two years, one year, and a month. Even
this T.MS refused ; Mohammed's sole concession was tliat
they should not be obliged to destroy their goddess witli
their own hands. The deputation retm'ned, and had nearly
reached TAif, when 'Abdyalil counselled the othera to make
as if they had broken off the negotiation, and not to con-
fess the conclusion of the pact till the Thalfif showed no
stomach for battle with Mohamm.cd. With faces covered,
like men who have no good news, they rode into the tovra,
and first paid the customary visit to the temple of the
Rabba. Then they told their tribesmen the conditions of
treaty, declared them intolerable, and reviled Jlohanimcd
as a hard and arrogant man. "And so," they concluded,
" pre)mro for war, lay in provisions for two years ;
Mohammed will surely not maintain the siege longer ;
dig a fosse to protect your stronghold, and lose no time."
Tiie Thal.cafitc3 at first agieed to this ; but in a few days
they lost courage, and bade the negotiators return and
accept the conditions. These then confessed the truth,
=* Non-Mof.lcra subjects were m.tde to p.iy nu nrbitrary cajiitntion or
incciiic tax.
' Tlie cxponiliture of this tax was regulated in tbe case of som«
tribes by ?i«*einl treaty.
^OHAKKKD.]
MOHAMMEDANISM
561
'•ad added that Mohammed's emissaries would presently
appear to destroy the Rabba. The destruction took place
accordingly, to the terror of the women and children, but
without a single man raising, his hand.
The pilgrimage undertaken by Mohammed in the. year
It) (March 632) was like a very triumph. All Arabia,
apart from the vassals of Persia and Greece, lay at his feet,
^e greatest success of his life had been effected by sheer
moral force without a stroke of the sword. But Arabia
no longer sufficed him ; he had wider aims. In his last
War years he began to extend th^ holy war against the Greeks.
<rtth the Even on his return from Hodaibiya, he began to direct
envoys to several foreign potentates, with letters demand-
ing their adhesion to Islam. One of these envoys was
seized and beheaded in the Belk& (the ancient Moab).
Hence sprang the first campaign against the Greeks, i.e.
the Arabs who were subject to the Greek empire. The
array directed against them was, however, entirely defeated
at Mu'ta (Autumn 629); Khilid succeeded with difficulty
in rallying and leading back the broken remnant of the
host. Next summer the Nabatseans who visited the mar-
ket of Medina spread a rumour that the Emperor Heraclius
■was collecting a vast force to attack the Moslems; and
Mohammed set forth to meet him at the head of 30,000
men, but got no farther than Tabiik, on the southern
borders of ancient Edom, when the rumour was found to
be false. The expedition, however, was not altogether
fruitless, as it led to the submission of several small Jewish
and (Christian communities in the north of the Peninsula.
Mohammed equipped a new expedition against the Greeks
on his return from his "farewell pilgrimage," and it was
Death just ready to start when he died, on Monday, 8th June
of Mo- 632.
natomed. jjj forming an estimate of one who has exercised so
unexampled an influence on the history of the world, we
shall do well to bear in mind the hint of Gibbon, that
" some reverence is surely due to the fame of heroes and
the religion of nations." The grounds on which Mohammed
may be condemned are partly found in his private life.
Although on the whole, even after he had become ruler of
all Arabia, he maintained the original poverty and simplicity
of his establishment, never set store by money and estate,
eating and drinking and soft clothing, strictly continued
to fast and watch and pray after his first fashi'^n, and that,
too, plainly out of a heartfelt need and without any osten-
tation, he nevertheless in one point at least used his supreme
authority as prophet to make provision for the flesh. He
claimed to be personally exempt from those restrictions in
regard to the female sex which lay upon all other Moslems,
and, as is well known, he made very extensive application
of this fundamental principle. This fact is quite rightly
urged against him as a reproach ; even pious Moslems have
been scandalised by it. At the same time, it is unnecessary
to judge him on this account more harshly than we do
Charlemagne, the most Christian king of the Franks ; in
any case we must not apply the standards of the present
day to the circumstances of old Arabia. Of much weightier
and indeed of crushing character is the accusation, that he
did not really believe himself to be a prophet, but merely
of set purpose played the part of one. For the first years
of lus activity indeed this charge is not now any longer
maintained ; it is universally granted that at that period
his enthusiasm was genuine and real But in Medina, we
are told, he used his prophetic character simply as a pretext
, for the establishment of his power. It seems to the present
writer that into this opinion there enter modem notions as
to the separation between religion and the civil magistracy,
which ought to be carefully kept out of sight. By any
other instrumentality than that of a prophet it would
hardly have been possible to found the slate of Medina ;
Its— 21
religion was the soul of the community. The founding of
a religion and the forming of a state were not connected
in 80 merely external a way as is usually supposed ; on the
contrary, the one was the natural and necessary consequence .
of the other. This must certainly be conceded,^hat, if Wft
are to make anj distinctions at all, Islam was far less rich
in religious meaning than in social forces. The Koran i»
Mohammed's weakest performance ; the weight of his
historical importance lies in his work at Medina and not
in that at Mecca. And it is a fact that the politician ia
him outgrew the prophet more and more, and that in inany
cases where he assigned spiritual motives he merely did so-
to give a fair appearance to acts that emanated fronusecular
regards. In this respect it appears to us particularly
objectionable that he gave out as revelations of God and
placed in the Koran aU sorts of regulations and orders of
the day, which proceeded simply from his own. deliberations'
or even in part were suggested to Iii'tti by advisers from'
outside. At the same time the element of self -.deception
is not excluded even here; he took for a message sent
down from heaven everything which in his cataleptic fits
passed through his mind, however close might be its agree-
ment with his own previously cherished thoughts. It was
pardonable that he went on with the idea after he had
once grasped it, that he blew upon the coals when the flame
threatened to die out. It ia less easy to free him from the
reproach of perfidy and cruel vindictiveness. The surprise
of Nakhla in the month Bajab (ordered by him, though he
afterwards repudiated it), the numerous assassinations
which he instigated, the execution of the 600 Jews at the
close of the War of the Fosse, burden the Prophet heavily,
and sufficiently explain the widespread antipathy in which
he is held. Yet even in this respect it is well not to forget
the instance, already cited, of Charlemagne. It is precisely
the man of vast aims who finds it most difficult to keep the
beaten path.
After the death of Mohammed arose the question who was
to be his "representative" (Khalifa, Caliph). The choice lay
with the community of Medina ; so much was understood ;
but whom were they to choose t The natives of Medina
believed themselves to be now once more masters in their
own house, and wished to promote one of themselves.
But the Emigrants asserted their opposing claims, and
with success, having brought into the town a considerable
number of outside Moslems,' so as to terrorize the men of
Medina, who besides were still divided into two parties.'
The Emigrants' leading spirit was 'Omar ; he did not,
however, cause homage to be paid to himself but to AbAlick
Ab\ibekr, the friend and father-in-law of the Prophet. Colipk.
The affair would not have gone on so smoothly, had no' Eevolt
the opportune defection of the Arabians put a stop to the "' *^»«
inward schism which threatened. Islam suddenly found '^""'•
itself once more limited to the community of Medina;
only Mecca and T^if remained true. The Bedouins were
willing enough to pray, indeed, but less willing to pay taxes ;
their defection, as might have been expected, was a political)
movement.' None the less was it a revolt from Islam, for
here the political society and the religious are identicaL
A peculiar compliment to Mohammed was involved in tha
fact that the leaders of the rebellion in the various districts
did not pose as princes and kings, but as prophets ; in this
the secret of Islam's success appeared to Lie.
Abilbekr proved himself quite equal to the perilous
situation. In the first place, he allowed the expedition
against the Greeks, already arranged by Mohammed, quietly
to set out, limiting himself for the time to the defence of
Medina. On the return of the army he proceeded to
• Compare Muir, iv. 253.
' See Noldeke, Beitr/tge mr Kenntniss dcr Pocsie der aiten Areiber
(1S64), p. 89 tq.
562
MOHAMMEDANISM
[ths first
attack the rebels. The holy spirit of Islam kept the men
of Medina together, and inflamed them to a death-defying
zeal for the faith ; while, on the other side, the Arabs as a
whole had no other bond of union and no better source of
Defi »! inspiration than universal egoism. As was to be expected,
rebela ^''^^ ""^^^ worsted; eleven small flying columns of the
Moslems, sent out in various directions, sufficed to quell
the revolt. Those who submitted were forthwith received
back into favour ; those who persevered in rebellion were
punished with death. The majority accordingly converted,
the obstinate were extirpated. In YamAma only was
there a severe struggle ; the Banil Hanifa under their
prophet Mosailima fought bravely, but here also Islam
triumphed.
The internal consolidation of Islam in Arabia was,
ifetrange to say, brought about by its diffusion abroad.
■The holy war against the border countries which Mohammed
lad already inaugurated, was the best means for making
the new religion popular among the Arabs ; for, in spread-
ing by means of the sword the worship of Allih, oppor-
tunity was at the same time afforded for gaining rich
booty. This vast movement was organized by Islam, but
the masses were induced to join it by quite other than
religious motives. Nor was this by any means the first
occasion on which the Arabian caldron had overflowed ;
once and again in former times emigrant swarms of
Bedouins had settled on the borders of the wilderness.
This had last happened in consequence of the events
which destroyed the prosperity of the old Sabiean king-
dom. At that time the small Arabian kingdoms of
Ghassin and Hira had arisen in the western and eastern
borderlands of cultivation ; these ntm presented to Moslem
conquest its nearest and natural goal. But inasmuch as
Hira was subject to the Persians, and Eastern Palestine to
the Greeks, the annexation of the Arabians involved the
extension of the war beyond the limits of Arabia to &
struggle with the two great powers.
KhAlid ia After the subjugation of Middle and North-Eastem
oynu. Arabia, KhAlid b. al-Walld proceeded by order of the
Caliph to the conquest of the districts on the lower
Euphrates. Thence he was summoned to Syria, where
hostilities had also broken out. Damascus fell late in the
summer of 635, and on 20th August 636 the great decisive
battle on the Hieromax (Yarmilk) was fought, which caused
the Emperor Heraclius finally to abandon Syria.' Left to
themselves, the Christians henceforward defended them-
selves only in Lsolated cases in the fortified cities ; for the
most part they witnessed the disappearance of the Byzan-
tine power without regret. Meanwhile the war was also
carried on against the Persians in 'Ir.^k, unsuccessfully at
BSitia first, until the tide turned at the battle of KAdislya (end
i>f KA of 637). In consequence of the defeat which they here
""J"*- sustained, the Persians were forced to abandon the western
portion of their empire and limit themselves to Eran
proper. The Moslems made themselves masters of Ctesi-
phon (Maddin), the residence of the Sasanides on the
Tigris, and conquered in the immediately following years
Ithe country of the two rivers. In 639 the armies of
Syria and "Irik were face to face in Mesopotamia. In a
short time they had taken from the Aryans all the prin-
cipal old Semitic lands,— Palestine, Syria, Mesopotamia,
Arar m Assyria, and Babylonia. To these was soon added Egypt,
Egypt, which 'Amt b. al-'As, aided by the national and confessional
antipathies of -the Copts towards the Greeks, overran with
litUo trouble in 641.^ This completed the circle of the
lands bordering on the wilderness of Arabia ; within
' Do Oocjf, ilinwiTes d'Hisl. el de Oiog: Orient., No. 3. Lcy'J*".
1864 : NUUieka, D. M. Z., 187C, p. 78 aqq.: Beladhori, 137.
• • See H. Zo'puberg in Journ. at., 18/ » (xiU. 2»l-386).^ The date
*• oerhf--" som." to<-» too ktOh
these limits annexation was practicable and natural, a
repetition indeed of what had often previously occurred.
The kingdoms of Ghassdn and Hira, advanced posts
hitherto, now became the headquarters of the Arabs ; the
new empire had its centres on the one hand at Damascuaj'
on the other hand at Cufa and Basra, the two newly
founded cities in the region of old Babylonia. The
capital of Islam continued indeed for a while to be Medina,
but soon the Hijdz and the whole of Arabia proper lay
quite on the outskirt of affairs.
It is striking to notice how easily the native populations
of the conquered districts, exclusively or prevailingly
Christian, adapted themselves to the new rule. Their
nationality had been broken long ago, but intrinsically
it W£is more closely allied to the Arabian than to the
Greek or Persian. Their religious sympathy with the
West was seriously impaired by dogmatic controversies;
from Islam they might at any rate hope for toleration,
even though their views were not in accordance with the
theology of the Emperor of the day. The lapse of the
masses from Christendom to Islam, however, which tooB
place during the first century after the conquest, is only to
be accounted for by the fact that in reality they had no
inward relation to the gospel at all. They changed theii"
creed in order to acquire the rights and privileges o6
Moslem citizens. In no case were they compelled to do
so ; on the contrary, the Omayyad CaUphs saw with dis'
pleasure the diminishing proceeds of the poll-tax derived
from their Christian subjects.
It would have been a great aavantage for the solidity
of the Arabian empire if it had confined itself within the
limits of those old Semitic lands, with perhaps the addition
of Egypt. But the Persians were not so ready as the Conqu'**
Greeks to give up the contest ; they did not rest until the "' ^f"-
Moslems had subjugated the whole of the Sasanid empire.
The most important event in the protracted war which led
'to the conquest of Eran, was the battle of NehAwend in
641 ;' the most obstinate resistance was offered by Persia
proper, and especially by the capital, Istakhr (Persepolis).
In the end, all the numerous and somewhat autonomous
provinces of the Sasanid empire fell, one after the other,
into the hands of the Moslems, and the young Shahanshah,
Yezdegerd, was compelled to retire to the farthest corner of
his realm, where he came to a miserable pnd.* But in mora
than one case the work of conquest had to bo done over
again : it was long before the Eranians learned to accept the
situation. Unlike the Christians of Western Asia, they
had a vigorous feeling of national pride, based upon
glorious memories Qud fispecially upon a church having a
connexion of the closest kind with the state. Internal
disturbances of a religious and political character and
external disasters had long ago shattered the empire of
the Sasanids indeed, but the Eranians had not yet lost
their patriotism. They were fighting, in fact, against the
desjiised and hated Arabs, in defence of their holiest pos-
sessions, their nationality, and their faith. They were
subjugated, but their subjection was only outward. The
commonwealth of Islam never succeeded in assimilating
them as the Syrian Christians were assimilated. Even
when in process of time they did accept the religion of
the Prophet, they leavened it thoroughly with their own
peculiar leaven, and, especially, deprived it of the practical
political and national character which it had assumed after
the Flight to Jlcdina. To the Arabian state they were
always a thorn in the flesh, it was they who helped rnosi
largely to break up its internal order, and it was fronJ
them also that it at last received its outward deathblow,
i!
' The occoiints diffor ; see Bel.idhori, 305. Tie chronolog;)- of thi
conquests, ft3 is wcti known, is in ni-iny points uncertaiji.
* Beladh., 315 tq. ; TaUnri, L 1068. .
MOHAMMEDANISM
i>G3
The fall ot the Oma/yads >ra3 their \roik, iixd with the
Omayyads fall the Arabian empire. The course of Islam's
political history during its first centuries is denoted by the
removal of th -, capital from, Damasctis to Cafa, and from
(Ma to Baghdid, the latter occupying, approximately, the
site of the ancient Ctesiphon.
But we must return to the period of Al- 'tiejir. Jde oied
after a short reign, on 22d August 634, dua ^■i matter of
course was succeeded by 'Omar. To 'Omar's ten years'
Caliphate belong for the most part the great conquests.
He himself did cot take the field, but remained in Medina ;
he never, hoT?ever, suffered the reins to slip from his grasp,
ao powerful WiS tJie influence of his personality and the
Moslem commimity of feeling. His political insight ia
shown by the circumstance that he endeavouied to limit
the indefinite extension of Moslem conque-it, and to main-
tain and strengthen the national Arabian cii^.racter of the
commonwealt;! of Islam ; * also by his making it his fore-
most task to promote law and order in its internal affairs.
The saying with which he began his reign will never grow
antiquated : '■ By God, Ije that is weakest among you shall
bo in my sight the strongest, until I have vindicated for
him his rights ; but him that is strongest will I treat as
the weakest, until he complies with the la^vs." It would
be impossible to give a better general definition of the
function of the State. ^ After the adminLstration of justice
he directed his organizing activity, as -the circumstances
demanded, chiefly towards financial questions — the incidence
of taxation in the conquered territories,^ and the applica^
tion. of the vast resources which poured into tbe treasury
at Medina. It must not be brought against him as a
personal reproach, that in dealing with these he acted on
the principle that the Moslems were the chartered plun-
derers of all the rest of the world. But he had to atone
by his' death for the fault of his system ; a workman at
Cufa, driven to desperation by absurd fiscal oppressions,
.stabbed him in thp mosque at Medina. He died in the
beginning of November 6ii.
IMore his.death 'Omar had nominated six of the leading
Emigrants who should choose the Caliph from among them-
scives— 'Othmin, 'All, Zobair, Talba, Sa'd b. Abl Walfki?,
and 'Abd al-RahmAn b. 'Auf . The last named declined to be
candidate, and decided the election in favour of 'Othm4n b.
'Affan. Under this weak sovereign the government of Islam
fell entirely into the hands of the Koraish nobility. We
havci already seen that Mohammed himself prepared the way
for this transference; Abiibekr and 'Omar likewise- helped
it ; the Emigrants -yeise unanimous among themselves in
tluaking that the precedence and leadership belonged to
thorn as of right. Thanks to the energy of Omar, they
■we;-o successful in appropriating to themselves the succes-
siOi! to the Prophet. They indeed rested the claims they
puo forward in the undeniable priority of their services to
tie faith, but they also appealed to their blood relationship
witli the Prophet, as a legitimation of their right to the
inheritance; and the ties of blood connected them with
the Koraish in general In point of fact they felt a
greater solidarity with these than, for example, -with the
natives of Medina ; nature had not been expelled by
faith.' The supremacy of the Emigrants naturally fur-
liished the means of transition to the supremacy of the
' He songht to make the whole nition a greot host of God ; the
Aiobs were to bo soldiers and nothing else. They were forbidden to
ecqi'.ire landed eatates in the conqnered countries ; all land was either
mode state property or was restored to the old owners subject to a
perpetual tribute which provided pay on a splendid scale for the army.
• Noldeko, Tabari, 2i6. To 'Omar also is due the estaWishnient of
thoEraof the Flight.
' Even in the list of the plain at the battle of Honain the Emigrants
lire enumerated alo"^ with tha Mtccans and Koraish, and disitngui^hed
from tlw men of ?decUn.<i,
Meccan ariatocracy. AJthmaii did a!! in his po-w*r to
press forward this development of affairs. He belonged
to the foremost family of Mecca, the Omayyads, and thaJ
he should favour his relations and the Koraish as' a whola
in every possible vray, seemed to him a matter of course.
Every position of iciiuence and emolument was assigned
to them ; they themselves boastingly called the import^!
province of 'Irrik th4 garden t)f Koraish. In truth, the
entire empire had become that gardei! Nor was it
unreasonable that from the secularization ~of Islam the
chief advantage should be reaped by those -who best knew
the world. Such were beyond all doubt the patricians of
Mecca, and after them those of T^if) people like Khilid b.
al-WaUd, 'Amr b.. al-'As, 'AbdaUAh b. AbX Sarh, Moghira
b. Sho'ba, and, above all, old Abii Sofydn With his spn
Mo'a-iviya, the governor .of Syria.
Against the rising tide of worldliness an opposition,
however, now began to appear. It ivas led by what may
be called the spiritual noblesse of Islam, wMch, as dis-
tinguished from the hereditary nobility of Mecca, might
also. be designated as the nobility of merit, consisting of
the " Defenders," and especially of the Emigrants who had
lent themselves to the elevation of the Koraish, but by no
means with the intention of r'lowing themselves to be
thereby erficed. The opposition -B-as headed by 'it]i,
Zobair; Talha, both as leadijag men among the Emigrants
and as disappointed candidates for the Caliphate, who
therefore were jealous of "Othmdn. Their motives were
purely selfish; not God's cause but their own, not
religion but power and preferment, were what they sought.*
Their party was a mixed one. To it belonged the men of
real piety, who saw -with displeasure the promotion to the
first places in the commonwealth of the great lords who
had actually done nothing for Islam, and had joined
themselves to it only at the twelfth hour, -n-hila those who
had borne the burden and heat of the day were passed by.
But the majority were merely a band of men -without
vievrs, whose aim was not a change of system but of
persons, that they themselves might fatten in the vacant
places. Everywhere in the provinces there was agitation
against the Caliph and his governors, except in Syria, where
'Othmin's cousin, Mo'4-wiya b, Abl SofyAn, carried on a
wise and strong administration, ^e movement was most
energetic in 'Irik and in Egypt. . Its ultimate aim was
the deposition of 'OthmAn in favour of 'All, whose o-wn
services as well as his close relationship tb the Prophet
seemed to give him the best claim to the Caliphate. Even
then there were enthusiasts who held him to be a sort ol
Messiah.
The malcontents sought to gain their end by force. Ir
bands they came from the provinces to iledii* to concuss
'Othmdn into concession of their demands. From the
Indus and Oxus to the Atlantic the world was trembling
before the armies of the Caliph, but in Medina he had
no troops at hand. He propitiated the mutineers by
concessions, but as soon as they had gone, he let matters
resume their old course. Thus things went on from
worse to worse. In the following year (656) the leaders
of the rebeb came once more from Egypt and 'IrAk to
Medina with a more numerous following ; and the Calipt'
again tried his former plan of making promises which he
did not intend to keep. But the rebels caught him in ^
flagrant breach of his word, and now demanded his abdi;
cation, besieging him in his own house, where he was
mcitt
a-^iinii
'C'.hJtuW
* It was the same opposition of the spiritual to the secular nobilltj
that afterwards showed itself in the revolt of the sacred cities against
the Omayyads. The movement triumphed with the elevation of the
'Abbasids to the tlirone. But, that the spiritual nobility was Sgbting
not for principle but for personal advantage was as apparent in 'All's
hostilities against Zobair and Tilha as in that of the 'Abbdsids agaisst
the follov-:^r; ^^f 'A3:.
564
MOHAMMEDANISM
[teb kastkbm
defended by a few faithful subjects. As he would not
yield, they at last took the building by storm and put
him to death, an old man of eighty. His death in the
act of maintaining his rights was of the greatest service to
liis house and of corresponding disadvantage to the enemy.
Controversy now arose among the leaders of the oppo-
sition as to the inheritance. The mass of the mutineers
summoned 'AH to the Caliphate, and compelled even Talha
and Zobair to do him homage. But soon these two, along
with 'Aiaha, the mother of the faithful, who had an old
grudge against 'AH, succeeded in making their escape to
'Irik, where at Basra they raised the standard of rebellion.
'All in point qf fact had no real right to the succession,
and moreover was actuated not by piety but by ambition
and the desire bf power, so that men of penetration, even
although they condemned 'OthmAn's method of govern-
ment, yet refused to recognize his successor. The new
Caliph, however, found means of disposing of their opposi-
tion, and at the battle of the Camel, fought at Basra in
November 650, Talha and Zobair were slain, and 'Aisha
was taken prisoner.
But even so 'All had not secured peace. With tho
miirdcr of 'Othmdn the dynastic principle gained the
twofold advantage of a legitimate cry — that of vengeance
for the blood of the gray-haired Caliph, and of a distin-
guished champion, the Syrian governor Mo'iwiya- Mo'Awiya
was not inclined to recognize 'All, and . the latter did not
venture to depose him. To have done so would have be-en
useless, for Mo'iwiya's position in Syria was impregnable.
The kernel of his subjects consisted of genuine Arabs,
not only recent immigrants along with Islam, but also
old settlers who, through contact with the Eoman empire
and the Christian church, had taken on a measure
of civilization. Through the Ghass&nids these latter
had become habituated to monarchical government and
loyal obedience, and for a long time much bett«r order
bad prevailed amongst tham than elsewhere in Arabia.
Syria was the proper soil for the rise of an Arabian
kingdom, and Mo'Awiya was just the man to make use of
the situation. He exhibited 'Othmin's blood-stained
garment in the mosque at Damascus, and incited his
Syrians to vengeance.
'Ah's position in Cufa was much less advantageous.
The population of Irik was already mixed up with
Persian elements ; it fluctuated greatly, and was largely
composed of fresh immigrants. Islam had its head-
quarters hero ; Cufa and Basra were the home of the
pious and of the adventurer, the centres of religious and
political movement. This movement it was that had
raised 'All to ^he Caliphate, but yet it did not really take
any personal interest in him. Religion proved for him a
much less trustworthy and more dangerous support than
did the conservative and secular feeling of Syria for the
Omayyada. Mo'iwiya could either act or refrain from
acting as he chose, secure in either case of the obedience
of his subjects. 'AH, on the other hand, was unable to
convert enthusiasm for the principle inscribed on his
banner into enthusiasm for his person. It was necessary
that he should accommodate himself to the wishes of his
supporters, and at the same time it was impossible, for
these wishes were inconsistent. They compelled him
suddenly to break oil the battle of SJiffln, which he was on
the point of gaining over Mo'dwiya, because the Syrians
fastened copies of tho Koran to their lances to denote
that not tho sword but the word of God should decide
the contest (end of July 657). But in yielding to the
will of the majority he excited tlio displeasure of the
minority, tho genuine zealots, who in Mo'iimj'a were
exposing the enemy of Islam, and who regarded 'All's
entering into negotiations with him as a denial of the
faith. When the negotiations failed and war was
resumed, the Khirijites refused to follow 'All's army,
and he had to turn his arms in the first instance against
them. He succeeded in disi)Osing of them without diffi-
culty, but in his success he lost the soul of his following.
For they were the true champions of the theocratic
principle ; through their elimination it became clear that
the struggle had in no sense anything to do ■with the
cause of God. 'AJfs defeat was a foregone conclusion,
once religious enthusiasm had failed him ; the secular
resources at the disposal of his adversaries were far
superior. Fortunately for him he was murdered (end
of January 661), thereby posthumously attaining an
importance in the eyes of a large part of the Mohammedan
world (ShI'a) which he had never possessed during his
life. His son Hasan made peace with Mo'ivriya.
The Khirijites are the moEt interesting feature of the'iio
then phase of Islam. In the name of religion they raised Kl^ir!-
their protest against allowing tho whole great spiritual ■'''**•
movement to issue in a secular and political result, iq the
establisliment within the conquered territories of an
Arabian kingdom, a kingdom which diametrically contra-
dicted the theocratic ideal. Islam was then on the point
of making its peace with the world, not -n-iihout a certain
apostasy from its original principles, for which Mohammed
himself had paved the way. Life was no more dominated
by religion, but came to tenns with it aud parted com-
pany. This development was favoxu-ed by the govern-
ment, which desired before all things to have peace.
Orthodoxy arose, and thereby religion was tamed and
divested of every dangerous element ; strictly speaking, it
became a compromise, according to which the letter of the
precept was correctly followed, in order that, in everj-thing
besides, a man might obey his ovnx inclinations. Tlie con-
ditions under which any one might make sure of heaven
were — on the one hand, the performance of " good works,"
i.e. of such opera operanda as had a special churcldy
merit assigned to them ; on the other hand, faith in tie
absolute soverfeignty of God even over the wills of men.
About morak G!od showed little concern — the usual view
of orthodox shamanism. This was by no means the
original standpoint of Islam, although the transition to
it was made at an early stage, and by the Prophet himself.
Originally Islam — i.e. religious resignation — was only the
complement of pious eJfort ; a man set himself about
even the hardest and apparently purposeless tafks, because
ho believed the issue to lie entirely in tho hand of God.
But now all this was reversed ; a man acted according to
his humour, because his destiny had nothing to do \rith
his inherent qualities, but was dependent entirely on
Allih's caprice. The Khirijites protested not merely
against the dynastic principle and the rule of the Omay-
yads, but also against orthodoxy ; they disputed the doc-
trine of predestination and the proposition that a great
sinner could yet bo a good Moslem, because they did not
understand how to divorce religjon from practice. To
some degree they call to mind the ~lSontanists, but their
opposition was much more energetic in its expression.'
Sources.— Yot the history of Mohammed these are— (1) the Son: est
Koran ; (2) the theologico-nistorical tradition or Hadith. Tlio
latter is chronologically arranged in the biographies, of which
those of Ibn Isliak and of AVakidi are the oldest aud most import-
ant. Ibn Ishak's work in ita complete form i^ now to be found
only in Ibn Hisham's revision (cd. Wilstcnfeld), but laigo and
numerous fra/^ments of the original are f,'ivcn by Tabari (ed. De
.long). Of W.ikidI the Kildb al-Maghiizi, i.e. the history of
Mohammed in Medina, is still extant (abridged German translation
by Wellhauscn, 1SS2) ; his coUcctiona for tho earlier period are
known to us through the work of Ibn Sa'd lus secretary {TaiaiM,
- On the further development of Islam compart Hontama, De Siri^
evtr ktt Zh/ma, Leyden, 187$.
•IXIP&iTE.]
MOHAMMEDANISM
565
ancdit«d). The Hidith is s«t forth more svstetnaticany, according
to subjecU. in the great collections of tradition by M^ik b. Anas,
Bokhari, Moelim, etc (Bulak editions). A subsidiary authority
i} the humanistic tradition of the Odaba, with which the poetry
luay be reckoned. The principal collections of thia class are the
KiUb al-Aghini (Bnlak edition) and the Kdmil (ed. Wright). For
the period after Mohammed the most important work is the
Chronicle of Tabari (Leyden edition) ; the history of the conquest
is treated briefly after the best authorities by Belidhorl (ed. Do
Goeje, 1866).
ZUerature. — The genuine tradition of the Arabs with reference
to their prophet was first introduced into Europe by the French,
beginning with Oagnier and ending with the valuable work of
CMWiin de PorceraL AVeil and, after mm, Noldeka especially, bare
the merit of haring shown how to om the Koran In coijunction with
the Arab tradition as a main source. Of modem biographiet the
most important are those of Jluir and Sprenger ; iwearch has not
yet got beyond them, although there is room foi this. For the
history of the Cahphs, the eUndard book is stiU the weD-known
work of Weil, although amce it waa published considerable addi-
tions have been made to our knowledge of tha sources, thank*
snecially to the Ubouia of Dozy, De Goeje, and other Dutchmen.
Hitherto the mam object has been to bring together the materiali
m this department of research, and a comprehensive treatment of
the entire subject has not as yet been accomplished ; still r«fereno«
may be made in this connection to Dozy {Hutoir, dt VIslnmime\
and A. von Kremer (Oesch. cUr herrxhmden Idem d. Itlam, and
KuUmrgachichU d. OrurnU xmter dm KhcUifen). (J wa)
PART IL— THE EASTERN CALIPHATE.
Sect. L — The Omayyads.
1. In commencing the history of the Omayyad dynasty
we mnst first recur to the causes which brought about the
triumph of this family, and which led its chief to substitute
£>amascu.s for Medina as the seat of the Caliphate ; an
event which led to profound changes in the Moslem empire,
and exercised a considerable influence on its development.
In the Game way, at a later date, the transfer of the Cali-
phate from Damascus to BaghdAd marked the accession of
a new family to the supreme power, and gave Islam a new
direction.
In the lime of Mohammed, the Arabs were divided into
an infinite number of tribes, some settled, others nomadic,
■which were conitantly at war with each other. The
Prophet united them into one body, but he could not
entirel}' eradicate the hatred v.hich had existed for ages
between tribe and tribe. Thus the people of Mecca and
those of Medina hated each other, because the former were
£ branch of the race of Ma'add, the great ancestor of the
tribes of the North ; ^ while the latter belonged to the
Yemenite race, or that of the South. The conquest of
Jlecca by Mohammed and his allies of Medina only exas-
perated this hatred, and the nobles of the Koraish swore
to take revenge on the Yemenites, as soon as they should be
able to do so. One of the most violent opponents of the
Prophet had been, as we have seen, the father of that very
Wo'Awiya who founded the Omayyad dynasty, Abii Sofyin,
grandson of Omayya, the leader of the Meccans in the battle
St Ohod ; and it is related that his wife Hind, having found
Hamza, Mohammed's uncle, among the dead, cut open his
body, and tore out and devoured his liver. We have also
i.j9ecn how Ab\i SofyAn ultimately made his submission and
embraced Islam, but only under compulsion. Wia eon
ilo'Awiya became, it is true, one of Mohammed's secretaries ;
but we know that his faith was never very strong, and that
he always made his religion subordinate to the interests of
his family. Even in his youth, he had conceived the project
of recovering the supreme power for his own race, and it
lias been related above how the inner conflicts of Islam
tinder the Caliphates of 'Othmin and "All carried him
forwards towards this goal
Mo'Awiya might, no doubt, have marched to the help
of 'OthmAn with an army of SjTians ; but the preserva-
tion of the Caliph, his relative, would not have served the
purposes of his burning ambition, and we may say with-
out hesitation that it was %vith secret joy that the prefect
of Damascus heard of the fatal result of the plot against
'Othmin. The Syrians were entirely devoted to Mo-
'iiwiya. Polite, amiable, and generous, he had gain* the
goodwill of all the Arabs of Syria, for whom Islam had
remained a dead letter, and who, continuing Bedouins at
heart, shared the feelings of their chief against the new
' The Ma'addites are aUo often called Mo4arites and KalwitA?, after
their asceston Mo^ar and K:iis.
aristocracy of Medina. Consequently, when 'All, 'Oth-
mAn's successor, summoned Mo'Awiyi for tha last time to
acknowledge him, and when Mo'A'^ya, assembling his
partisans in the mosque of Damascu.-!, asked their advice,
they replied that it was his part to command, and theirs
to obey and to act. The enthusiasm of the Syrians waa
great ; and Mo'Awiya having ordertd a levy en massf,
within three days every able-bodied man had joined his
standard. Syria alone supplied Mo'Awiya with more
troops than all the rest of the pronnces put together
furnished to 'AH, who is said to have a Idressed his soldiers
with these bitter words : " I would gbdly eschange ten of
you for one of Mo'Awiya's soldiers." Then he added — in
allusion to the savage action of Hind, Mo'Awiya's mother,
on the field of battle at Ohod — " By God ! he will gain
the victory, this son of the liver-eater 1 "
'All's gloomy anticipations were fulfilled ; but it was by
stratagem that Mo'Awiya gained his victory. The battle
of Siffin, the abortive negotiations that followed, and the
withdrawal of the KiArijites, have been already spoken of.
The negotiations ended in the conference of Dfimat al-
Jandal, a small place situated between Syria and 'IrAJf,
about seven days' journey from Damascus and thirteen
from Medina. Here in Ilamadan, A.H. 37 (a.d. 657-658),
Abii MisA and 'Amr b. al-'As (the famous conqueror of
Egypt) appeared as arbitrators for 'AH and Mo'Awiya
respectively, and the cunning of the latter induced Abu
MiisA to pronounce both pretendants deprived of whatever
rights either might have to the Caliphat-e, and to say that
it now rested with the Moslems to make a new choice.
'Amr, who waa only waiting for this declaration, rose in his
turn, and said to the Arabs who were crowding round the
platform : " O people, ye hear what Al^ii MiisA says. He
himself renotmces the claims of his master. I also agree tj
the deprivation of "All, but I proclaim my master Mo'Awira Mo'i-
Caliph." Abii MiisA cried out against this treachery, but *^y* '•
no one would listen to him, and he fled for refuge to
Mecca, where he ultimately recognised the claims of
Ho'Awiya, even in 'All's lifetime. This event marks the
commencement of the Omayyad dynasty. 'Amr weat in
triumph to Damascus, where the Syrians took tha wth of
fidelity to Mo'Awiya.
In 'IrAk, on the other hand, with the exception of the
Khirijites, all thr people remained fsithful to the cause
of 'All, who, mounting the pulpit at (Jufa, summoned his
army to the field, and fixed their rencezvous at Nokhaila,
a sinall place not far from the city. The Kharijites had
taken refuge at NahrowAn, and 'Aii found it necessary to
attack them there, before marching against the Syiiana.
At his arrival most of the rebels d'spersed, except from
fifteen to eighteen hundred fanatics, who remained at
their post and allowed themselves to be slaughtered to
the last TTiftTi Thus rid of tha Kh.irijites, 'Ali meant to
direct his march towards Syria, but his soldiers refused
to moTO, and declared their intenticn of first taking soine
066
MOHAMMEDaNIS
[oilATTADft
rest at Cufa, Compelled to inaction, 'Alf returned to
Cufa, while Mo'iwiya gave his attention to securing the
possession of tho iiroviuces. At tlio beginning of a.h. 38
(a.d. 658-059), Egypt was lost to 'Alt 'Anir b. oJ-'As
was sent thither by Mo'Awiya, and marched vrithout
delay, at the Load of five thousand men, against "All's
vicegerent, Mohammed, son of the late Caliph, Abiibekr.
The brave general Ashtar, whom 'Ali sent to the help of
Mohammed, was poisoned at Kolzom by the prefect of
that place, acting under secret orders from Mo'dwiya, and
'Ali's troops retraced their steps. Meanwhile, in Egypt
itself, a partisan of the Omayyads, Mo'Awiya b. Hodaij,
who was at the head of six thousand fighting men, had
declared against Mohammed, and driven him from Fostit.
On his arrival in Egypt, "Amr effected a junction with
Mo'dwiya b. Hodaij, and the unfortunate Mohammed,
beaten by his adversaries, fell into the hands of Ibn
Hodaij, who put him to death.
While Egypt was thus being lost to 'All, commotions
were excited at Basra itself by a partisan of the Omayyads.
These were, however, put down by the governor of that
city, Ziyid. This man was Mo'iwiya's own brother, but
illegitimate, and not having been acknowledged by his
father, Abil SofyAn, he had revenged himself by embracing
the party of 'Alt Ziyild was renowned among the Arabs
fcT his eloquence, his resolution, and his courage. At a
later period, Mo'iwiya gained him over to his cause by
publicly acknowledging him as his brother. At the time
we speak of, he was a faithful servant of 'AH, and as soon
as the revolt of Basra was put down^ he marched into
Firsistan, where he maintained peace and kept the
inhabitants in their allegiance. Meanwhile, however, the
other proWnces were falling one after the other under the
power of Mo'Awiya, His generals penetrated into the
heart of Chaldasa ; and even in Arabia, where 'All's
generals had at first gained some advantages, Bosr ' b.
'Artah obtained possession of Medina a.h. 40 (a.d. 660-C61),
and compelled its inhabitants to acknowledge Mo'Awiya.
After this he marched upon Mecca^ expelled Kotham,
'AU's governor, and there also exacted an oath of obedience
to his master. Following up his successes, Bosr did not
hesitate to press southward, and soon gained possession
of Yemen. 'All was nov,' no longer master of anything
but 'Irak and a part of Persia, and even of these provinces
the former vfas menaced by the Syrians, as we have seen.
Taking advantage of some partial successes gained by his
forces in Arabia and in Syria, 'All made overtures for
peace, but they were rejected. Mo'4wiya believed himself
too sure of ultimate success to be willing to share the
(empire.
It was then that three men of the Khirijites conceived
the project of delivering Islam from those who were
desolating it with fire and blood. 'Abd al-Rahm4n b.
Moljam, Boraik b. 'Abdallah, and 'Amr b. Bekr agreed
that on the very same day the first should kill 'All at Cufa,
tlie second Mo'ilwiya at Damascus, and the third 'Amr b.
al-'As at FosUt. They fixed on Friday the 15thof Ramad.-tn,
A.H. 40,- when they were sure of finding their victims at
K^Msi- the mosque. The plot was put in execution, but 'All
wiion of along fell. On the appointed day, Boraik made his way
'■ into the mosque of Damascus, and stabbed Mo'Awiya in
the back with his sword. Before he could repeat the
blow he was seized, and Mo'Awiya recovered from his
wound. As for 'Amr, he had been kept at home by
Illness ; his place at the mosquo was fakeu by KhArija,
the chief of his guards ; and it was he who fell beneath
the blows of 'Amr b. Bekr. 'Abd al-Rahmin was more
' Not liishr, a» sc
brtrua aear li.wa»
:^ liistorians call him. Bosr pave his name
. Bt-ladhori calls bim Bour k. Abi Arlih.
EucceasfuL As 'All was entering the mosque, he dealt bim
a blow on the head with his sword, and stretched him on
the ground mortaUy wounded. Two days later "Alf died,
and the assassin was put to death with horrible torments.
'All left two sons, Hasan and Hosain. The people ol
Iri^ chose Hasan Caliph. But he, not having his father's
energy, recoiled before the prospect of a war with
Mo'iwiya. Though he had an army of forty thousand *
men at his disposal, he preferred to renounce the Caliphate.
Besides, one of his generals, Kais b. Sa'd, who had urged
him to continue the struggle, and had himself tried tha
chance of arms, had just been beaten by the Syrians. In
consequence of this defeat, a mutiny had broken out in
Hasan's army. He abdicated, and only demanded, in
exchange for the power which he resigned, pardon for his
relatives and a yearly pension of five millions of dirhems,^
together with the revenues of the Persian city of Ddrib,
gird. A treaty to this effect was concluded between
Mo'dwiya and Hasan, in spite of the opposition of Kosaln,
who exhorted his brother to continue the straggle ; and
Mo'iwiya entered Cufa at the head of his army, accord-
ing to some authorities towards the end of the month of
Rabf I., A.H. 41 (July, a.d. €61), according to others a
month or two later. Hasan retired to Medina, where he
died eight or nine years afterwards, poisoned, it is said,
by order of the Caliph.
Mo'Awiya, who now remained sole master of the Jtcslem ilo'i-
empire, was, however, not yet univertaU}' acknowledged. >''y»
Five thousand Khirijites made head against him in the ^°'^ ..
province of AhwAz, the ancient Susiana, and a revolt broke
out at Basra. Ziydd himself, Mo'dvriya's brother, refused
to take the oath to him, and fortified himself at Istakhr,
the ancient Persepolis. The revolt it Basra was put down
by Bosr b. ArUh, and Moghfra b. Sho'ba, whom Mo'iwiya
had named prefect of Cufa, accepted the task of bringing
about a reconciliation with ZiyAd. Ziy.ld refused to taka
the oath of allegiance only because he feared being called
to account for certain sums of money which were missing
from the public treasury of Persia. Mo'iwiya promised to
shut his eyes to these irregularities ; and ZiyAd came to
Damascus and was very well received by the Caliph, who
hastened to adopt the liastard as his brother, to the great
scandal of all pious Moslems.^ After acknowledging ZiyAd,
who thus became ZiyAd son of Abii SofyAn, Mo'Awiya
entrusted him with tho government of Basra and of Persia,
and afterwards with that of Cufa, when !Moghfra b. Sho'ba
died. ZiyAd governed 'IrA'if with the greatest vigour, to
tho full satisfaction of Mo'Awiya, who further placed the
whole of Arabia under his authority ; but in that same
year, a.h. 53 (a.d. 672-673), ZiyAd died. It seems that
Mo'Awiya had thought of him as his successor in the
Caliphate. After ZiyAd's death, the Caliph wished tc
secure tho throne for his o^vn son Yazid. This was a new
violation of tho customary rights of Islam ; for Mohammed,
whoso actions served as a rule, had not in his lifetime
appointed any one as his successor. Mo'Awiya, who was a
statesman .iboye everything, and who held religion very
cheap when it interfered with his objects, did not hesitate
to create a precedent.. He met, however, at first with
vigorous opposition, and it was not till some ye.irs later
that ho ventured to liave his intentions publiily announced
from the pulpit. In Syria the people took the oath o)
allegiance to Yazid ; in Arabia and 'IrAV ]iuMic opinion
declared itself against the step which Mo'Awij-a had taken.
^ Tho dirbera is a silver coin \vorth about o franc.
' At a later period, th« Abbasid Caliph Mahili thoiiglit it riBht tc
havo the names of Ziyad and bis descendants struck off the rolls of the
Koraisb : but, after bis death, the persons concerned gained over the
chief of the rolU. office, .ind gx)t their names replaced oa the li^ts. fcct
Tabari, iii. 479.
OMATVADS.]
MOHAMMEDANISM
567
The Cnliph Tas not moved ; threats prevailed over the
obstinacy of the people of "Irilj, and Mo'dwiya repaired to
Arabia in person, at the head of an army, to intimidate the
inhabitants of Mecca and Medina. As may bo supposed,
the principal fo'mentera of tho resistance in Arabia were
the sons of the first Caliphs,- "Abd al-Ealimin the son of
Abiibekr, 'Abdalliih the son of 'Omar, and Hosain the
son of 'Ali ; for, by submitting, they would have renounced
all hope of being themselves chosen by the people. Another
"Abdallih, son of that Zobair who had been among the
six candidates nominated at the death of 'Omar for tho
choice of the Moslems, was also one of the wannest
opponents of the pretensions of Mo'iwiya. AH the efforts
of the Caliph to win over these personages to his side
lianng proved vain, he ordered them to be brought into
the mosque at Mecca, each between two soldiers ; then,
having mounted the pulpit, he called on tho bystanders to
take the oath of allegiance to his son ; adding that 'Abd
al-Ralun4n, Hosain, and the two 'AbdallAhs would raise no
objection. They, in their terror, did not utter a word, and
the assembly took the oath. Then Mo'Awiya, without con-
cerning himself further about the malcontents, returned to
Damascus.
Wliile thus occupied at home, Mo'iwiya did not neglect
foreign affairs. 'Amr b. al-'As, governor of Egypt, died
x.n. 43 (A.D. 663-664), and was followed by several prefects
in succession, under one of whom the general Mo'dwiya b.
Hodaij undertook several expeditions into the province
of Africa. In the year 50 (a.d. 670) he advanced as
far as Camunia, now Siisa, near which city he laid the
foundations of the celebrated Kairawin, and even went
on to Sabaratha, a town situated near the seashore, and
opposite to the island of C'rina. The emperor, Constiintino
IV., had sent thither thirty thoxisand Greeks, who were
beaten and compelled to re-embark in haste. Mo'awiya b.
Hodaij returned to Egypt after his victory, and the Caliph
now considered the jiosition of the Moslems in Africa so
strong, that he separated that province from Egypt, and
appointed as governor of Africa 'Okba b. Nifi', who per-
manently established Kairaw4n, in a plain situated at a
little distance from the first encampment of Mo'Awiya b.
Hodaij. -According to some historians, the new city .was
completed A.H. 55 (a.d. 674-675).
In the East the successes of the Moslems were still more
brilliant. Ziy.W, brother of Mo'Attiya, as soon as he was
aiipointed governor of 'IrAlf and Persia, sent an army into
IChorisAn. It advanced as far as the Oxus, crossed that
river, and retiirned loaded with booty taken from the
wandering Turkish tribes of Transoxiana. BokhirA was
occupied by a son of Ziydd, and Sa'd, son of the Caliph
'Ofhinin, whom Mo'Awiya had made governor of IChorasAn,
marched against Samarkand, A.H. 56 (a.d. 675-676).
Other generals penetrated as far as the Indus, and over-
ran and conquered MiiltAn, K4b>ilistdn, Mokrin, and
Sijistiin.
In the North the Moslems were not less fortunate in
their attacks on the Byzantine empire. Mo'Awiya, while
still only governor of Syria, had gained possession of
Armenia, and had sent a fleet against Cyprus, which, in
conjunction vrith that of the governor of Egypt, had
effected the conquest of that island. Encouraged by the
result of this expedition, he gave the order for new incur-
sions in the Mediterranean. His fleet of twelve hundred
vessels invested the islands of Cos, Crete, and Rhodes.
The famous Colossus of Rhodes was broken to pieces, and
it is said that the bronze of which it was made was bought
by a Jew of Emesa, and formed a load for nine hundrpd
and eighty camels. The Arabs even dared to threaten
Constantinople, which owed its safety only to the Greek
fire. Tazld. the son of Mo'iwiya, took part in these
expeditions, but with no great ardour, and in the year 58
(a.d. 677-678) Mo'iwiya concluded a thirty years' peac«
with Constantine IV. Two years later, he died at Damas*
cus, after a reign of nearly twenty years. He had been
governorof Syria for the same length of time. Before hia
death, he sent for his son Yazld, and having pointed out
how he had smoothed down all difficulties for him, he
advised him to spare no effort to preserve the attadiment
of the Syrians. He urged him also to keep a close watch
on the actions of Hosain b. 'AU, and of the other pre-
tenders who had refused to take the oath of allegiance to
him ; but he added that, should they rebel, Yazid ought
to treat them with clemency, and not to forget their illus-
trious origin. By failing to act upon this wise advice,
Yazld rendered irreconcilable that formidable schism which,
even at the present day, still divides the Moslem world,:
and which, at all neriods, has been a source of calamity to
Islam.
2. Yazfd had not his father's jrenius. Passionately Yadd I.
fond of pleasure, and careless about religion, he bestowed
more care on turning a pretty couplet than on consoli-
dating the strength of his empire. During his short reign
he committed three actions for which Moslems never
pardoned his memory : the murder of Hosain, son of 'AM
and grandson of the Prophet ; the pillage of Medina ; and
the taking of the Ka'ba, the venerated temple of Mecca ;
crimes which were not redeemed in the eyes of the people
by a few fortunate expeditions on the part of his generals.'
Immediately on ascending the throne, in the month
Rajab a.h. 60 (April, a.d. 680), Yazld sent a circular to all
his prefects, with an ofiicial announcement of his father's
death, and an order to administer the oath of allegiance to
their respective subjects. In particular, he charged the
now prefect whom he appointed to ifedina, his own cousin
Walid b. 'Otba, to strike off the heads of Hosain son of |
'All, 'Abd al-Rahmin son of Abiibekr, 'AbdalUh son of
'Omar, and 'AbdallAh son of Zobair, if they again refused
to acknowledge him. Terrified at such a commission,
Walld did not dare to act with rigour against Hosain and
'AbdalUh b. Zobair, both of whom refused to take the
oath, but allowed them to escape to Mecca. Yazldj
immediately deprived him of his office, and appointed inl
his place 'Amr b. Sa'ld, already governor of Mecca. Oncet
in the Holy City, "AbdalUh b. Zobair thought himself inu
such perfect safety that he began to intrigue with tha
Meccans to have himself proclaimed Caliph in ArabiaJ
At Cufa the news of the flight of Hosain produced greafl
agitation among tho partisans of the famUy of 'All, who*
were numerous there, and they sent several addresses tdf
the grandson of tho Prophet, inviting him to take refuge!
with them, and promising to have him proclaimed Calipht
in 'Irdk. Hosaiu, who knew the fickleness of the people'
of 'Irdk, hesitated to yield to their entreaties ; but Ibn.
Zobair, who was desirous to get rid at all costs of so
formidable a rival, persuaded him that he ought to go
and put himself at the head of the people of 'Irdk, and'
enter on an open struggle with Yazld. Hosain began by
sending his cousin Moslim b. 'AkH to Cufa, and from himj
he learned that many of the inhabitants of that city:
appeared really decided to support him. The prefect ofi
Cufa, No'mAn b. Bashlr,- though apprised of these pro-!
ceedings, did not choose to make them known to Yazld,]
as he was reluctant to act with severity against a descend-]
ant of the Prophet. Information, however, reached the
Caliph, who deprived No'min of his office, and ordered^
' Salam b. ZiyiA invaded Sogdiana, and brought back immense*
booty to Merv. In Africa 'Okba b. Ndfi' invaded the whole coast ofj
the Mcditsn-anean as far as Morocco. On his return, however, hej
fell into an ambuscade laid by the Berbere, who killed him and tooM
Ksiraviii.
568
MOHAMMEDANISM
[oMATTASat
febaid All4h, son of the famous Ziydd, and then governor
pt Basra, to give up hia post there to his brother 'Othmdn,
and to repair in person to Cufa, in order to watch the
■partisans of "All in that city. 'Obaid Allih obeyed,
entered Cufa, and, ascending the pulpit the very day after
his arrival, publicly announced his firm intention of putting
to death any one who should rebel Moslim b. "AljO was
given up by a traitor and executed. Meanwhile Hosain,
on receiving his cousin's despatches, had already set out
from Mecca with all his family, and had reached KAdisiya
(a place situated only fifteen parasangs ' from Cufa, and
noted for the defeat sustained there by the Persians
daring the Caliphate of 'Omar), when he received the
tews of these vexatious occurrences. He wished to
retrace his steps immediately, but the friends of Moslim
dissuaded him from doing so, crying out for revenge,
and representing to liim that doubtless he had only to
show himself under the walls of Cufa to be received with,
enthusiasm by its inhabitants. Hosain accordingly pur-
sued his journey towards Cufa. But "Obaid Allih, who
was watching all his movements, sent four thousand
liorsemen, devoted to the Omayyad cause, to meet him,
»with orders to bring Hosain before him either alive or
dead. The commander of. these horsemen was 'Omar b.
Sa'd,^ to whom 'Obaid Allih had promised the govern-
ment of Media as a reward, if his expedition should
succeed. The Omayyads met Hosain iu the plain of
febSi. Kerbeli, opposite to Cufa, before he had reached the
4)upirates, and surrounded him. 'Omar b. Sa'd himself
sought out Hosain and summoned him to surrender.
Sosain declared himself ready to renounce his pretensions,
provided he were allowed to return to Mecca with his
followers, or were even sent to Damascus. When 'Obaid
Allih was informed of this proposal, he simply repeated
iis former order to bring Hosain to Cufa, dead or alive ;
and, fearing the defection of 'Omar b. Sa'd, he sent out
another troop of horsemen under the orders of a certain
•Shimr. On the 9th of Moharram in the year 61 (9th
October a.d. 6S0), Shimr reached Kerbeli, and summoned
Hosain afresh to surrender at discretion. Hosain pre-
ferred to die sword in hand, and on the following day,
after a desperate struggle, he was cut down with all his
followers. His head was cut off and carried to Cufa, and
then sent to Damascus. His body was not buried till
the following day. Only the women of his family were
spared, and one of his sons ; these were taken by Yazld's
order to Medina, where the sight of their mourning and
the tale of their sufferings caused a profound sensation.
The horror and grief of the partisans of 'All's family were
great. Hence tiie nanies of Yazld, 'Obaid Allah, and
'Shimr, have been held accursed ever since by the Shi'ites..'
fehey observe the 10th of Moharram as a day of public
Irnouming. Among the Persians, stages are erected in
public places on that day, and plays are acted, represent-
ing the misfortunes of the family of 'Alt* The Omayyads
themselves were loud in their reprobation of this impious
massacre, and all Moslems, without distinction of party,
considered it a monstrous act.
,At Mecca the news was received with a degree of
indignation of which 'Alxlallih b. Zobair took advantage to
assume the title of Caliph. As early as A.H. 60, the new
prefect of Medina had tried to secure his person. He had
sent against him a force of two thousand men, at whose
* The parasang is nearly equivalent to an English milo,
' Son of tho famous Sa'd b. AW WakkiU, conqueror of Persia
undei 'Omar, and founder of Cufa.
,• Shi'ites comes from Shi'a, a word which In Arabic signifies "seo-
tary." It is the name given to the partisans of tho family of 'AH,
,who acknowledge no legitimate Caliphate*^ outside of that family.
'Shi'ism is the religion of Persia.
* reeChodzko, r/Kfdtrejwsan. Paris, 1878.
head w^a3 placed a brother of the pseudo-Caliph himself,
called 'Amr, who, having been accused by 'Abdallih of
maintaining a guilty intercourse with one of his wives,
had become his bitter enemy. 'Abdallih collected ao
army, and placed it under the orders of 'Abdallih b.
Safwin, who completely defeated the Omayyad troops.
The brother of the pseudo-Caliph was taken apd put to
death. At the news of this defeat, Yazld swore that
Ibn Zobair should never appear before him but as a
prisonc. in chains. He dismissed the new prefect of
Medina, and reinstated Walld b. 'Otba, who, in the year
61, went to Mecca to try to seize 'Abdallih b. Zolteir.
The latter, in derision, wrote to Yazld : " WaUd is a mad-
man, who will ruin everything by his folly ; send in his
place another governor to repaiir the wifongs he has done."
Yazld thought that "Abdaliih meant these words as a step
towards reconciliation ; hastened to deprive Walld' of his
office ; appointed 'Othmin b. Mohammed in his place ;
and even sent envoys to Ibn Zobair. He, however, would
not listen to them ; he thought he could reckon upon the
devotion of the people of Mecca, 8jid further hoped that
Medina itself would declare against Y'azld. This, in fact,
took place in the year 63 (a.d. 6S2-683). The people of
Medina, stirred up by a certain 'Abdallih b. Hanzala,
who had had a near view of Yazld at the court of Damas-
cus, and had been scandalized by the profligacy of his life,
revolted, drove the governor and all the Omayyads out of
Medina, and proclaimed the dethronement of Yazid. The
Caliphate was even offered by some to 'All, that one of the
sons of Hosain who had escaped the massacre of Kerbeli ;
but 'All wisely refused it. At the news of this revolt^
Yazfd first sent an ambassador to Medina. This step
proving fruitless, he next collected an army of from ten
to twelve thousi^d Syrians, and entrusted their command
to Moslim b. "Olfba, who passed, and with good reason,
for a man who would recoil from nothing. This general,
though weighed down by age and sickness, marchfd
against Medina, took it, after a, battle known as the day of
Harra ' (26th Dhi '1-Hijja 63, 26th August 683), and gave
up the city for three days "to massacre and pUlage. Tor-
rents of blood flowed, and hence Moslim b. 'Ofcba received
the surname of Mosrif (the Prodigal). On the fourth
day, Moslim repaired to the mosque, and received the
oath of allegiance from all those of the citizens of Medina
who had not been able to make their escape. The news
reached Mecca a few days later, a»J fell like a thunder-
stroke on Ibn Zobair aud his adhetents, who prepared for
war, expecting from day to day to see Moslim appear
before the waUs of their city. He had, in fact, started
for Mecca immediately after the conquest of Medina ; but
he died on the road, and the command was taken by
.Hosain b. Nomair. The Omayyad army arrived before
Mecca a month after the capture of Medina, and fotmd
ribn Zobair ready to defend it. A number of the citizws
of Medina had come to the aid of the Holy City, as well
as many Khirijites and Shi'ites, at the head of whom was
a certain Mokhtir b. Abi 'Olxiid, who subsequently
played a very important part in 'Irili:. In spite of the
sorties of the Meccans, tho Syrian army invested the city.
Hosain b. Nomair had caused balistas to be placed on
the neighbouring" heights ; and these, under the manage-
ment of an Abyssinian soldier, hurled against the Ealia
enormous stones and vc.<«els full of blazing bitumen, with
such effect that the temple took fire and was consumed.
After a siege of two months, Ibn Zobair was beginning
to despair, when he received, through an Arab of the
desert, news of the death of Yazld. The Caliph had in
fact died on the IBth of Rabf I. (11th November 683).
Csp-.u.-o
.-:.d pil-
Slrge or
Mecca.
* Ilarra is the volcanic district outside of Slodiaa. One of tho
gates of the city is called tho Cote of Harra.
OUATYASe.]
MOHAMMEDANISM
569
Hosain b. Nomair inunediately offered the Caliphatpe to
Ibn Zobair, on condition that he should grant a complete
amnesty to all those who had taken part in the battle of
Harra and in the siege of Mecca. 'AbdallAh had the folly
to refuse, and Hosain then returned to Damascus.
ibn Zo- Thus rid of his enemy, 'AbdalUh caused the title of
hair pro- Prince of the True Believers (Amir al-mo'minin) to be
"''''i"^ conferred on him — a title which 'Omar had already
^"^;^, received, and which was afterwards adopted by all the
Uev«rs„ Caliphs. He sent one of his brothers, "Obaid Allih, to
Medina, and chose as. governor of Egypt 'Abd al-RahmAn
b. Jahdam, who repaired to that province, and caused the
authority of Ibn Zobair to be acknowledged there. At
Basra and at Cufa, many of the inhabitants did not
hesitate to acknowledge him, and received a Zobairite
governor, while the Kh4rijites and the Shi'ites rose in
revolt — the former at Basra under the leadership of Nifi"
b. Azrat, the latter at Cufa under that of SolaimAn b.
gorad — and expelled the Omayyad governor, 'Obaid
All.ih b. Ziyid, who took refuge at Damascus. Mesopo-
tamia soon followed the example of 'Irdfe. Even in Syria,
the population seemed disposed to forsake the cause of the
Omayyads. The Klulrijites and Mokhtir b. Abl 'Obaid,
who had supported Ibn Zobair, now repented of having
laboured for the elevation of this pretender, and quitted
Mecca. The son of Zobair, remaining thenceforth sole
master of Mecca, occupied himself tranquilly in rebuilding
the Kalia, which he restored on its ancient foundations.
Uo'iwl- 3. It was in the midst of this bre^-up of his party
y« U. that, immediately after the death of Yazid, his eldest son,
Mo'dTviya IL, was elected Caliph at Damascus at the age of
only seventeen or twenty. He. was a young man of weak
character, and imbued, it is said, with Shl"ite opinions.
He felt himself incapable of ruling, and was contemplating
abdication, when he died, after a reign of but forty days,
by poison, as some say ; of the plague, as others assert.
The Caliphate was immediately offered to 'Othmdn b.
"Otba b. Abi Sofyin, cousin of Mo'iwiya IL ; for KhiUid,
the second son of Yazld, was only sixteen years old.
'Othmin b. "Otba, however, having made it a condition of
his election that he should not be compelled to enter on
any war, or to condemn any one to death, the choice fell
at Damascus on Merwin b. al-Hakam, a descendaiit of
Omayya through his grandfather Abtl l-'As, but on con-
dition that he should marry Maisiin, the widow of Yazld,
and should appoint Khilid, her son, as his successor.
MorwCn 4. MerwAn b. al-Hakam had been secretary to the
L Caliph "Othmin, and governor of Medina under Mo'Awiya
L Yarld, on his accession to power, had dismissed him
and put Walld b. "Otba in his place ; but MerwAn had
continued to live at Medina, and had been driven from it
duiihg the revolt of the year 63, and again in the following
year, when "Obaid AllAh b. Zobair had taken possession
of that city in the name of his brother. It might have
been thought that Merwin would cherish a deep hatred
of "Abdallih Ibn Zobair ; but he was an old man of sixty-
two at the time of his election, and, dreading an unequal
struggle, he was on the point of making his submission to
the Meccan Caliph. The drooping courage of Merwin was
revived by his son 'Abd al-Melik and by "Obaid Allih b.
Ziydd, and he resolved to try the chances of war.
Dahbik b. ICais, governor of Damascus, had declared
himself on the side of Ibn Zobair, and had raised an army,
principally from among the tribe of Kais. This tribe had
taken offence because Mo'imya I. and Yazld had chosen
their wives from the Yemenite tribe of Kalb, and, con-
tinuing to resent their conduct, now refused to acknowledge
Khilid as the heir-presumptive of Merwin. It was there-
fore on the Yemenites that Merwin had to depend for the
suppression of Dahhik's rebellion. The latter had an
le— 21*»
'army of nearly sixty thousand horsemen, while Merwin
could bring together only thirteen thousand infantry.
The two armies met at Marj Rihit, a few miles from
Damascus, and, after a series of combats which lasted for
twenty days, Merwin's troops gained a complete victory,
and Dahhik was among the killed. The Syrian provinces
hastened to acknowledge the conqueror, and Merwin was
able to turn his attention to Egypt, which, as will be
remembered, had submitted to the Meccan. 'Abd al-
'Azlz, a son of Merwin, had already marched to Aila on
the Bed Sea, and was preparing to enter Egypt ; Merwin
joined him, and the Zobairite governor of Egypt, beaten
by their united forces, was obliged to seek safety in flight
Merwin made 'Abd al-'Azlz governor of the province. At
the beginning of the year 65 (a.d. 684-685) Merwin
returned in haste to Sjrria; for, during his absence, a
brother of Ibn Zobair, named Mos'ab, had invaded that
province. Merwin triumphed over Mos'ab ; but an army
of four thousand men, which he had sent to the Hijiz,
and in which was Hajjij b. YTisuf — then quite a young
man, but who afterwards played so important a part xmder
"Abd al - MeUk — was cut to pieces. This defeat was
redeemed by a victory gained by his generals, "Obaid
Allih b. Ziyid and Hosain b. Nomair, at "Ain al-Warda
over a small army of Shi'ites led by Solaimin b. Sorad.
But whOe the battle was being fought in Ramadan 65
(April-May 685), Merwin died ; suffocated, it is said, by
his wife Maisiin, because he had insulted her son Khilid,
and had broken his word by nominating his own son
'Abd al-MeUk as his successor. The accession of 'Abd al-
MeUk was attended with no difficulty, as he was acknow-
ledged by the whole of Syria and Egypt. The Kaisites
naturally rallied round him, because he had not a drop of
Yemenite blood in his veins.
6. When 'Abd al-Melik ascended the throne, there still" AM i*
remained much to be done before the unity of the empire "^'^l*-
could be re-established. Ibn Zobair was still master of
Arabia and of "Irik, though in the latter province hia
authority was very much shaken by the permanent rebel-
lion of the Shi'ites at Cufa, and of the Khirijites at Basra.
The Zobairite general Mohallab had, it is true, succeeded
in forcing back the Khirijites into Susiana and Persia;
but at Cufa the Shi'ites, at the instigation of Mokhtir,
continued their agitation. Mokhtir, as we have seen, had
vrithdrawn from Mecca after the raising of the siege by
Hasain b. Nomair. He returned to Cufa, and there
fomented serious disturbances. Many of the inhabitants
of that city repented bitterly of having allowed Hosain,
the grandson of the Prophet, to be massacred. Amid the
general disorder of the Moslem empire, Mokhtir hoped
to make his own authority acknowledged in 'Irik and
Mesopotamia. Se put himself forward as the avenger of
the family of 'All, and pretended to have been commissioned
by a son of "All, Mohammed b. Hanaflya,^ who was living
at Medina, to give effect to his rights to the Caliphate.
Many Shlftes believed him, and, detesting their chief
Solaimin b. Sorad, joined Mokhtir. On learning these
intrigues, the Zobairite governor threw him into prison.
Soon after the defeat of Solaimin at "Ain al-Warda, at the
request of Mokhtir's brother-in-law, who was no other
than "AbdaUih the son of "Omar, the governor consented
to set him at liberty, on his swearing to make no further
attempts against hiim. As Solaimin had fallen on the
' That is to say, the son of the Hanafite woman. Tlio mother of
Mohammed was of the tribe of Hanifa. Even before Mokhtar, Mo-^
hammed had partisans who looked on bim as destined to be Caliph.
These sectaiies received the name of Kaisinites, from a freeduinn of.
'AM, called Kaisin, who was the most ardent advocate of Moliammed'»J
pretensions. After Mokhtir bad declared in favour of Mohamme4,^
his supporters received the name of Mokhtirite.s.
570
MOHAMMEDANISM
[OMAYYIDS.'
field of battle at '^Un al-\Varda, all the Shi'ites now'
acknowledged Mokhtir as their > chief. He, however, con-
sidering himself bound by his oath, remained inactive
until the governor who had imposed it was replaced by
'Abdallih b. Moti". The new Zobairite governor, suspect-
ing with reason that Mokhtir was about to recommence
his intrigues, thought it advisable to invite him to his
house, with the intention of having him arrested. Mokh-
tilr called his partisans together, and plotted with them to
take Ibn Moti' by surprise. As, however, Sa'd, one of the
Shl'ite chiefs, asked for a delay of a week, for the purpose
of collecting troops, Mokhtdr was obliged to feign illness
in order to evade the governor's invitation, and took care
to surround himself with a numerous body of guards.
Meanwhile Sa'd, who had only demanded this delay iu
order to ascertain the real wishes of Mohammed b. Hana-
fiya, sent off four confidential messengers to Medina, to ask
Mohammed whether he had really confided the care of his
interests to MokhtAr. Mohammed contented himself with
replying vaguely that it was the bounden duty of every
good Jloslem to take part with the family of the Prophet.
These words were interpreted in favour of Mokhtir, and
thenceforward all the Shi'ites followed him blindly as
their chief. Mokhtir fixed the middle of the month
Eabi' I., A.H. 66, for the commencement of hostilities.
During the night of the 13th to the 14th, the conspira-
tors intended to gain possession of the city by a coup
de main/ but the governor was on his guard, and
Revolt of Mokhtir and his Shi'ites took the course of leaving Cufa.
Mokhtir They numbered sixteen thousand resolute men. All the
armies which "AbdaUih b. MotC sent against them were
successively beaten, and Mokhtir soon re-entered Cufa in
triumph, compelling the Zobairite governor to flee to Basra.
Once master of Cufa, Mokhtir thought himself already in
possession of the empire. He sent emissaries to Medina,
to Mosul, to Madain, and even into Azerbaijin, with
orders to induce the people to take the oath of allegiance
to him. He then sent his generals, Yazid b. Anas and
Zofar, against the Omaj'j'ad army, which had entered
Mesopotamia after the battle of 'Aan al-Warda, and these
prevented the advance of the Syrians into 'Irilf. Another
of Mokhtir's generals, Ibrihira b. MiUk, inflicted a serious
defeat on the Syrians near Mosul, and 'Obaid Allih b.
Ziyid, who commanded them, fell in the battle. n)rihlm
■was rewarded by Mokhtir with the government of Mosul.
Mokhtir himself next took the title of " lieutenant of the
Mahdl " ' and inserted in the Kholha, on Friday's preaching,
a prayer on behalf of Mohammed b. Hanaflya ; which was
equivalent to declaring him Caliph. After this, urged on
by his adherents, he caused all those who had taken part
in the mas.sacre of Hosain, the grandson of the Prophet,
like 'Omar.b. Sa'd and Shimr, to be sought out and put to
death.
While these events were occurring, the Caliph at
Damascus, "Abd al-Melik, sent an army of observation to
the frontiers of Arabia. Mokhtir, having been informed
of this, feigned an intention to help Ibn Zobair, and de-
spatched a body of three thousand men from Cufa, under
the command of a certain ShariUl. His real object was
to concentrate forces at Medina, with a view to attacking
Ibn Zobair. But the latter penetrated his design, and two
thousand Meccans marched by his orders to meet Sharihll,
who was defeated.
In the same year (a.h. 66) Mohammed b. Hanafiya had
gone to Mecca to perform the ceremonies of the pilgrimage.
^ Mahdi, or " the wcll-giiided," is the name given by the ShCites to
that member of the family of 'Ali wlio, according to their belief, is oac
day to gain possession of the whole world, and set up the reign of
righteousness in it. In Mokhtilr'n tine, Mobiunmcd b. Hauafiya was
looked upon as the Mahdi.
Ibn Zobair took advantage of tliis to seize his person, and
confined him in a small house adjoining the well of Zamzam,
within the precincts of the Ka'ba. Mohammed succeeded
in conveying intelligence of his detention to Mokhtir ; and
he, delighted to find his aid implored by the very man
whose follower he called himself, swore to effect his rescue.
He despatched a thousand chosen horsemen, who managed
to conceal their march so well, that they were under the
walls of Mecca before the son of Zobair had been able to
make the slightest preparations for defence. They made
their way into the Holy City; but, being iin-ivilling to
draw the sword on that .sacred ground, they armed them-:
selves with sticks, broke in the doors of the house in which
Mohammed b. Hanaflya was imprisoned, rescued him, and
escorted him out of the city. A son of Mohammed, called
'.iVlf, who had also been thrown into prison, likewise suc-
ceeded in escaping, and rejoined ids father at some distance
from Mecca.
In the following year, Ibn Zobair, who was detennined
to get rid, at all- costs, of so dangerous an adversary as
Mokhtir, ordered his brother Mos'ab to elTcct a junction
with MohaUab, the conqueror of the Khirijites, and to
march against Cufa. ilos'ab and Mohallab invested that
city, and Mokhtir, making a sortie against them, was
beaten, taken prisoner, and beheaded. 'Irik thus, for Peath of
the second time, fell under the rule of Ibn Zobair. Jlokhtir.
Ibri'iirn b. Milik, who held Mosul in the name of
Mokhtir, submitted to the conquerors, on condition of
retaining his government ; but Mos'ab deprived Lini of
lus office, and put Mohallab in his place. He himself
was appointed governor of 'Irik; by his brother, and,
having installed himself at Basra, placed Cnfa under the
orders of bis lieutenant Hirith. The year after, the
Khirijites of Susiana raised a frash insurrection, xind
invaded 'Irit Mohallab had to be recalled from Mosid,
and during his absence it was Ibr:ihlm b. Milik whom
Mos'ab chosa to supply his place. The period of the
pilgrimage caused a momentary tnice to all these struggles,
and in that year was seen the curious spectacle of four
different standards planted near Mecca, belonging respe<t
tively to four party chiefs, each of whom was a pretender
to the empire : the standard of "AbdoUah b. Zobair,
Caliph of Mecca ; that of the Caliph of Damascus, 'Abd
al-Melik ; that of the son of 'All, Mohammed b. Hanafiya ;
and that of the Khirijites, who were at thai, time under
the command of Najda b. 'Amir. Such, however, was
the respect inspired by the holy places, that no disorders
resulted from the presence of so many inveterate rivals.
The Omaj-j'ad Caliph, whose troops had been beaten
in Mesopotamia, and who had been hitherto content to
watch the frontiers of Arabia, was again prevented from
pushing on military operations more actively by tho
breaking out of troubles in Syria. At the beginning
of A.H. 69 (a.d. 688-689), 'Abd al-Melik having left
Damascus at the head of a numerous army, with the
purpose of marching against 'Irik, the Oniayyad 'Amr b. 'Amr k
Sa'id, whom he had appointed governor of Damascus, took Said,
advantage of his absence to lay claim to the supreme power,
and to have himself proclaimed Caliph by his partisans.
'Abd al-Melik was obliged to retrace his steps, and to lay
siege to his own capital. The garrison of Damascus took
fright, and deserted their posts ; so t'lat 'Amr b. Sa'id,
abandoned by his followers, was compelled to surrender at
discretion. 'Abd al-Melik at first meant to spare him, but
he afterwards changed his mind, and strack off his head
with his own hand. Scarcely had he suppressed this revolt,
when the Emperor of Con.stantinople, Justinian II., in viola-
tion of the thirty years' truce formerly concluded between
Mo'Awiya I. and Consl;antine PV., sent a Greek army to
invade. Syria. 'Abd al-Molik was obliged to buy peace
KOMAYV.VDS.]
MOHAMMEDANISM
571
jDcond
fdege of
Ueco3.
/or the time, for he required all his forces to dispute the
empiro with the son of Zobair. He consented, it is
tisserted, to pay the Greeks an indemnity of one thousand
pieces of gold weekly. He then gave his attention to the
renewal of the projected expedition against 'IrAfc Mos'ab
the 2k)bairite had rendered himself odious to the inhabit-
ants of Basra and Cufa by his exactions, and a party
favouriible to 'Abd al-MeUk was already forming in those
cities. The Omayyad Caliph marched forth at the head
of an army composed of Syrians and Egyptians, and
encamped three parasangs from the plain of Dair al-
Jithalik, not far from the site of Baghdid, where Mos'ab
had established his army. Before joining battle, 'Abd al-
Melik had written secretly to all the chiefs of Mos'ab's
army, making them the most seductive promises if they
would agree .to desert the cause of Mos'ab. This step was
crowned with success, and on the eve of the battle, which
took place on the 13th Jom4df II., a.h. 71 (23d Nov-
ember 6D0), several of these generals passed into the
amp of 'Abd al-Melik with arms and baggage. Mos'ab
nevertheless attacked his enemy, but during the battle he
found himself deserted by his troops, and, not choosing
to survive his defeat, he caused himself to be ,ilain. This
victory opened the gates of Cufa to 'Abd al-Melik, and all
'Irdlj: X'oceived him with acclamations. He remained forty
days at Cufa, and then, having given the government to
his brother Bishr, while Khdlid b. 'Abdallih received that
of Basra, ho returned in triumph to Damascus. Soon
after, the Omayyad arms having sustained a check from
the Kh.irijites in Fdrsistin, the Caliph gave Khilid orders
to march against those sectaries ^vith the support of
Mohallab, who was their terror, and of the governor of
Eey. Khilid succeeded completely in this expedition,
and drove the Khirijites out of AhwAz, Firsistiin, and
Kirmiiu. On his side, the Omayyad Caliph stirred up a
revolt in Khorisdn, a province which still remained faithful
to the Zobairite cause. Its governor was treacherously
assassinated by his lieutenant Bokair, who received, as the
price of this service, the governorship of the province.
Only Arabia now remained to Ibn Zobair. In a.h. 72
'Abd al-Melik made preparations for depriving him of it.
Accordingly he raised an army; but when his generals
found that another siege of Mecca was in contemplation,
not one of them was willing to accept such a mission. An
obscure officer, Hajjdj b. Yi'isuf, boldly offered to lead the
expedition. 'Abd al-Melik had little confidence in him,
and therefore at first placed only two or three thousand
horsemen under his command. Hajjdj set out, traversed
the Hijiz without resistance, and pitched his camp at T^,
not far from Mecca. Ibn Zobair tried to dislodge him ;
but in the frequent encounters between his troops and
those of HajjAj, the latter always had the advantage.
'Abd al-Melik then decided on sending him a reinforcement
of five thousand men, on receiving which Hajjij invested
Mecca. The blockade lasted several months, during which
the citj' was a prey to all the horrors of siege and famine.
Hajjaj had set up balistas on the neighbouring heights,
and poured a hail of stones on the city and the Ka'ba.
Famine at length triumphed over the last adherents of the
son of Zobair. Ten thousand fighting men, and even
several of the sons of the pretender, left the city and
surrendered. Mecca being thus left without defenders,
HajjAj took possession of it and invested the Ka'ba. Then
the son of Zobair, seeing that ruin was inevitable, went to
Ids mother AsmA, who had reached the age of a hundred,
and asked her counsel. She answered that he must die
sword in hand ; and when, in embracing him for the last
time, she felt the cuirass which he wore, she exclaimed
that such a precaution was luiworthy of a man resolved to
jierish. 'AbdallAh tool: oif his cuirass, and taking refuge in
the Ka'ba, passed the night there in prayer. At daybrr:ik of
the 14th of Jomidl L in the year 73 (Ist October 692),
the Omayyad troops made their way into the mosque.
'Abdallih attacked them furiously, notwithstanding his
advanced age, but at last fell, overwhelmed by numbers.
His head was cut off, carried to HajjAj, and sent by the
victorious general to Damascus.^
With Ibn Zobair perished the influence which the early
companions of Mohammec' had hitherto exercised over Islam.
Medina and Mecca, though they continued to be the Holy
Cities, had no longer the political importance which had
enabled them to maintain a struggle with Damascus.
Temporal interests, represented by Damascus, will hence-
forth have precedence over those of religion ; policy will
outweigh fanaticism ; ^ and the centre of Islam, now per-
manently removed beyond the limits of Arabia, will be
mora easily affected by foreign influences, and assimilate
more readily their civilizing elements. Damascus, Cufa,
and Basra will attract the flower of all the Moslem
provinces ; and thus that great intellectual, literary, and
scientific movement which is to reach its apogee under the
'Abb.feid Caliphs at Baghdid, will become daily mora
marked.
By the death of the son of Zobair, 'Abd al-Melik
remained sole Caliph; for Mohammed b. Hanafiya
reckoned for nothing since the death of Mokhtir, whose
creature he had been. The only remaining danger was
from the Kidrijites, who, though incessantly repulsed, as
incessantly returned to the charge. HajjAj had remained
after his victory at Mecca, wlere he was occupied in
rebuilding the Ka'ba, ruined for the second time by his
engines of war. In the year 75, 'Abd al-Melik, alarmed
at the news which reached him from Persia and IrAk,
named HajjAj governor of that province, and gave him the
most extensive powers for the re-establishment of order.
The troops of "Ir4k, 'who accompanied Mohallab in an
expedition against the Khdrijites, had abandoned their
general and dispersed to their homes, and nothing could
induce them to return to their duty. Hajjaj, arriving
ilnexpectedly at Cufa, ascended the pulpit at the moment
when the people were assembled for morning prayers, and
delivered au energetic address to them, which depicts his
character so well, that some passages from it may be
cited : —
■"Men of Cufa, I see tofore me heads ripe for the harvest, and
the reaper — I am he I I seem to myseff already to see blood
between turbans and shoulders. I am not one of those who can
be frightened by an inflated bag of sHn, nor need any one think
to squeeze me like dried figs. I have been chosen on good
grounds ; and it is because I have been seen at work that I have
been picked out from among others. The Prince of the Believers
has spread before him the arrows of his quiver, and has tried every
one of them by biting its wood. It is my wood that he has found
the hardest and the bittorest, .^nd I am the arrow which ho shoots
against you."
Thereupon Hajjij ordered that every man capable of
bearing arms should immediately join Mohallab in Susiana,
and swore that all who made any delay should have their
heads struck oS. This threat produced its effect, and
HajjAj proceeded to Basra, where his presence was followed
by the same restdt. Mohallab, reinforced by the army of
'IrAk, at last succeeded, after a struggle of eighteen
months, in subjugating the Khirijites, and was able, at
the beginning of A.H. 78, to return to HajjAj at Basra.
The latter loaded bim with honours and made him
'AW al-
Melik
Caliph.
Hajjill ib
'irik.
^ On these events, see Quatremfere, Memoirs hi^torique sur la fj>
(TAba-AUah b. Zobair. raris, 1832.
' It is said that the Caliph "Abd al-Melik aOTected great piety before
his elevation. At the moment when he was fir.^t saluted with the title
of Caliph, ho closed a copy of the Sorun which was in his hands, say*
ing : *' We must now part."
672
MOHAMMEDANISM
[OMAYYADS.
governor of Kliorisin,^ whence he directed several expedi-
tions against Transoxiana.
■WTiilo Mohallab was fightbg against the Khirijites in
Persia, Hajjdj himself had had to struggle against rebel-
lion. Three Kliirijites, Silili, Shablb, and Motarrif, had
succeeded in creating a party in Mesopotamia and 'InSt
The second had even pushed his audacity so far as to
march upon Cufa, and for a moment had occupied that
city. Hajjij overcame the rebels ; and through his
vigilance, Katarl b. al-Foj.i'a, another KhArijite chief, after
being pursued as far as Xabaristan, on the Ca!.-pian Sea,
■was taken and killed by two Omayyod generals.
When he gave the government of Khorisin to Mohallab,
HajjAj had committed that of Sijistdn to 'Obaid AllAh b.
Abi Bakra. At the beginning of a.h. 79, 'Obaid Allih's
troops were beaten by the king of Kibill. Hajj^ th'ought
it advisable to remove 'Obaid Allih and to replace him
by the captain of his guards, 'Abd al-Ralimin b. al-Ash'ath,
rbn ol- This was a bad choice, for Ibn al-Ash'ath had often given
Atli'at!'.. proofs of an insubordinate temper, and Hajj^ soon had
occasion to repent of it. In fact, soon after his arrival
in Sijistin, 'Abd al-Rahmin, whose army was composed
of contingents from Cufa and Ba-sra, always ready for
revolt, conceived the design of an insurrection against the
authority of Hajjaj. Popular movements often go beyond
iho object first proposed; and not only did the troops
welcome joyfully the idea of marching against the hated
governor of 'Iri^ but they even proclaimed the dethrone-
ment of 'Abd ai-MeUk, and saluted Ibn al-Ash'ath as
Caliph. The new pretender entered Firsistin and AhwAz,
and it was in this last province, near Shuster, that
Hajjdj came up with him, after receiving from Syiia the
reinforcements which he had demanded in all haste from
the Caliph. Hajjdj was beaten and obliged to retreat.
Ibn al-Ash'ath pursued him as far as Basra, which opened
its gates to bim ; but fortune soon changed, and he
■was again driven out by his adversary. Ibn al-Ash'ath
tl'.en turned his arms against Cufa, and ■with aid from
■nithin, obtained possession of it; thus cutting the com-
munications of Hajjdj ■with Syria. The latter, thus com-
pelled to leave Basra, took the field, and pitched his
camp at Dair al-Jamdjim, two days' journey from Basra.
Ibn al-Ash'ath marched against him at the head of his
army. The condition of 'Irdlf caused the greatest uneasi-
ness at Damascus, and 'Abd al-MeUk hoped to stifle the
revolt by proposing to the insurgents the dismissal of
Hajjdj from his post The insurgents rejected this offer,
and hostilities recommenced. At the end of three months,
in Jomidf IL, A.n. 83 (July 702), a decisive action
took place. Victory declared for Hajjdj. Ibn al-Ash'ath
fled to Basra, where ha managed to collect frefh troops ;
but, having been again l>eaten, he took refuge in Susiana,
from which ho was driven by a son of Hajjdj. The rebel
then retired into Sijistin, and afterwards sought an asj^jn
■with, the king of KdbiiL As soon as Ms partisans had
rejoined him, he penetrated into Khordsdn, in order to
raise an insurrection there. The governor of tiiis province
was at that time Yazld, son of the celebrated Mohallab,
who had died in the year 82. Yadd marched against
Ibn al-Ash'ath, and cut his ormy to pieces. From that
time the pretender disappeared ; and it is thought that,
having again taken refuge ■with the king of Kdbiil, he
was betrayed by him and put to death.' It was duiing
' In A.H. 78, 'Abd al-Melik had made KhorisdnandSijistan depend-
ent on the governor of 'Iriik, so that Hajjdj had the right of directly
Don.inating the go'/emora of those provinces
' Thia king of KAbdl is called RatbCl or Rotbil by some historians,
»nd Zenbfl by others. See 'Weil, OeschuJilt dfr Chali/en, i. HO;
Tabari, trinsl. by Zotenberg, iv. 127 ; and Mas'iidi, transl. by Barbier
de Meynard, index, t. v. KotbU. According to Abulfeda's Oeography,
this long struggle tnat, in the year 83, Hajjaj«-!ai.l the
foundations of the city of "VV'dsit (the Intermediate) ; bo
called because it is situated midway between Cufa and
Basra. Some time after the suppression of this revolt, in
the year 84, Hajjdj deprived Yadd b. Mohallab of the
government of Khordsdn, accusing him of partiality
towards the rebels, and appointed in his stead first his
brother Mofaddal b. Mohallab, and nine months after
Kotaiba b. Moslim, who was destined at a later period to
e.xtend the sway of the Moslems in the East as far as
China.
VSTiile these events were taking place, 'Abd al-MeUk Progwta
■was engaged in the West in a struggle against the Greeks, of *^
We have seen that in the year 69 the Caliph, compeUed ^^'"
as he then was to direct all his eflbrts towards 'L-alf and
Arabia, had concluded a disgraceful peace with Justinian
IL It ■was not till A.n. 73 (a.d. 692-693) that he
resumed hostilities in Armenia, Asia Mmor, and Africa.
The operations in Asia Minor and in Armenia were
entrusted to Mohammed b. Merwdn, brother of the Caliph,
and to 'Othmdn b. Walld. They beat the Greeks at
first ; but, in consequence of subsequent reverse^ the
Moslems were compelled to accept peace, which iv&s
broken anew by the Greeks about the year .75 or 76, the
Caliph in one of his letters to Justinian IL having used
expressions which displeased the Christian monarch. In
retaliation, Justinian threatened to have legends offensive
to Islam struck on his coins. As, up to that tune, the
Moslems had no special coinage of their own, and princi- Tirst
pally used Byzantine and Persian money, this menace led Ar^W*
'Abd al-MeUk to institute a purely Arabic . coinage. It
was a Jew of Taimd, named Somair, who commenced its
fabrication. Justinian IL refused to receive these coins
in payment of the tribute, and declared the treaty at an
end. The incensed Moslems fought valiantly, and 'suc-
ceeded in extending their frontiers to Mar'ash, on the
side of Asia Minor, and to Amid, on the side of Armenia.
From this time forth the Moslems made yearly expedi-
tions against the Greeks ; but they were only razzias, for
which the Greeks often avenged themselves by incursions
into the territory of Lslam.
In Africa we have seen that 'Olfba b. Ndfi' had been
slain hy the Berbers, who had taken Kairawdn. In tlie
year 73 'Abd al-Melik sent Kassdn b. No'min into
Africa, at the head of a numerous army. He retook
Kaira^n-dn, swept the coast as far as Carthage, expelling
the Greek garrisons from all the fortified places, and
then, turning his arms against the Berbers, beat them so
completely that they submitted for a long time to the
tribute and the conscription. But when Hassdn left Africa,
the Greeks, under the successor of Justinian, retook the
ccast-line. Hassdn prepared to return to Africa, but he
previously demanded from the governor of Egypt, 'Abd
al-'Azij, the recall of a freedman, whom he had appointed
governor of a part of the province of Africa. 'Abd al-
'A^ij. refused, and Ha.ssdn went to Damascus to complaifl
to the Caiiph. Soon after his arrival at the capital he
died, and the governor of Egypt placed MilsA b. Nosair
at the head of the expedition. This general reconquered
the seaboard as far as Carthage, rjjd drove the Greeks
permanently from it. The daring Miisd continued his
triumphant march, and took possession of the whole of
the coast to Tlcmcen. One of his lieutenants, in tha
year 82, carried a reconnaissance by sea as far as Sicily.
The Moslem fleet having been destroyed by a storm,
Musd equipped another, and entrusted its command to his
brother 'AbdaUdh, who returned to Sicily and effected a
coinag*!
p. 343, rbn al-Asli'ath was killed in the province of Arrokhaj (Ai7&<
chosin), and bia bead waa sent to Damafciu and E^pt
jSUAYYADS.]
MOHAMMEDANISM
573
Tfizzia there. MerwAn, the father of 'Ahd al-ilelik, had
dcsigiiated as successor to the latter his other son, 'Abd
fcl-'Azfz, governor of Egypt. 'Abd al-'Aziz having died
in the year 84, 'Abd al-Melik; chose aa heirs of the empire,
(first his son Walid, and after him hia second son Solaiin4n.'
He himself survived "Abd a"l-'^.2iz only two years, and
(died 14th Shawwil 86 (8th October 705), at the age
of about sixty. His reign was one of the most unquiet
in the annals of Islam, but also one of the most
glorious. "Abd al-Melik not only brought triumph to the
cause of the Omayyads, but extended ani strengthened
the Moslem power externally. ' Amid so many grave
anxieties, he yet found time for his pleasures. He was
pa'5sionately fond of poetry, and his court was crowded
■with pijcts, whom he loaded vrith favours, even if they
■were Christians, like AkhtaL In his reign flourished
also the two celebrated rivals of Akhtal, Jarir and
Farazdalj:.'
Wslfd I.' 6. Immediately on his accession Walid confirmed
Hajjilj in the government of "IrAfe, and appointed as
governor of Medina his cousin 'Omar b. 'Abd al-'Azlz, ■who
■was received there wiUi joy, his piety and gentle character
being well known. Under his government important
■works ■were undertaken at Mediaa and Mecca by order of
■WaUd, who, having no rivals to struggle against, was
able to give his attention to pacific occupations. The
mosque of Medina was enlarged, wells ■were sunk, the
streets widened, and . hospital! established. At Mecca
many improvements were introduced. The reputation of
'Omar attracted to the two Holy Cities a great number of
the inhabitants of 'Irik, who were groaning under the iron
hand of HajjAj. The latter, ■who was not a man to let his
prey escape from his grasp, was so urgent ■with WaUd
that he obtained the dismissal of 'Omar b. 'Abd al-'Aziz in
the year 93, and the appoiatment of 'OthmAn b. Hayydn
at Medina, and of Khilid b. 'Abdallih at Mecca, These
two prefects compelled the refugees at Mecca and Medina
to return to 'Irilf, •where many of them were cruelly treated
and even put to death by HajjAj. It ■was probably his
craelty which drove so many men of 'IrAlf to enlist in the
armies of the East and the South ; and this may in some
degree account for the unheard-of successes of Kotaiba b.
Moslim in Transoxiana, and of Mohammed b. KAsim in
India. They may also be explained by the ambition of
Hajjiij, who, it is said, cherished the project of creating
a vast empire for himself to the east and south of the
Moslem realm, and had secretly promised the government
of China to the first of his generals who should reach that
' country. Be this as it may, in the coiirse of a very few
years Kotaiba conquered the whole of Bokharia, KhArizm,
and Triinsoxiana or MA ■warA-annahr, as far as the frontiers
of China. Meanwhile Mohammed b. KAsim invaded
MokrAn, Sind, and Miiltdn, carried o£f an immense booty,
and reduced the women and children to slavery. In
Armenia and Asia Minor, Maslama, brother of the Caliph
WaUd, and his lieutenants, also obtained numerous suc-
cesses against the Greeks. In Armenia, Maslama even
advanced as far as the Caucasus.
On- The most important achievement, however, of Walld's
W»«t reign ■was the conquest of Spain. The narrative of this
rfSpain. conquest belongs specially to the history of Spain ; and we
shall therefore only touch briefly on it here. We have seen
that, even in the Caliphate of 'Abd al-Melik, MiisA b.
Nosair had penetrated as far as Tlemcen in Africa. Under
"Walid, MiisA, who had been appointed governor of Africa,
entered Morocco, occupied Fez and Tangier, and then
* 'Abd al'McIik had several other sons, tv.-o of whom, Yaad und
Bi3ham, also reigned.
' Sea Caniaio de Perceval, Journal asiaiitiM, 2* eerie, vols. xiii.
and zir.
returned to KairawAn, having made his lieutenant TAriV
governor of Tangier and of all the West of Africa. The
town of Ceuta still held out under its governor Julian,
who held it in the name of Witiza, ICing of Spain. Witiza
having been dethroned by Roderic, Julian thought he
might find the Arabs usefxU allies in the struggle ■which
he proposed to carry on against the usurper ' and entered
into negotiations vrith Tirik. The latter, foreseeing the
possibility of conquering for the advantage of the Arabs a
country which had been represented to him as a paradise,
requested instructions from MiisA, who referred the matter
to the Caliph. WaUd gave MiisA carte blanche, and TArik
hastened to malce aUiance ■with Julian. He first, however,
sent four ships, ■vrith five hundred men under the command,
of Tarlf, to reconnoitre the coimtry. This expedition was
successful, and TArik, now. certain of meeting no serious
opposition to his landing, passed into Spain himseU, at the
head of twelve thousand men, in the year 92 (a.d. 710-711),
and landed at the spot which thence received the name of
Jabal-TArik, or " Mountain of TArik," a name which ■was
afterwards corrupted by the Westerns into Gibraltar. At
the nevra of this invasion, Roderic led a numerous army
against the Arabs, but was completely routed near Cadiz,
and perished in the conflict. MisA, jealous of the
success of his lieutenant, hastened to Spain ■with eighteen
thousand men, and his first step on arriving ■was to send
TArik orders to suspend his march. But T^rik, far from
obeying, divided his Uttle army into three corps, and
obtained possession successively of Ec\ja, Malaga, Elvira,
Cordova, and Toledo. MusA, hopeless of arresting the
victorious march of T^rik, determined to play the part of
a conqueror himself, and took Seville, Carmona, and
Merida, On rejoining TArik at Toledo, the first step .he
took ■was to throw him into prison. The CaUph, how-
ever, gave orders that he should be set at liberty and
restored to his command. The two conquerors then
shared the country between them, and, in less than
three years, all Spain' was subdued, to the very foot of
the Pyrenees. Mean^while WaUd, fearing to see MiisA
declare his independence, recalled him to Damascus. He
obeyed after appointing his son 'Abd al-'Azlz governor of
Spain, and assigning Se^viUe as his residence. MiisA left
Spain in the month of Safar, a.h. 95 (October-November
713), in company ■with T^rik, bringing an immense booty to
Damascus, and leading in his train a great number of
prisonei-s. His journey from Ceuta to Damascus was
one long triumpk He reached Egypt in the month of
Rabl' L in the following year (Nov.-Dec. 714), and then
moved on by short marches to^wards Damascus, where he did
not arrive till two months and a half later, at the very
moment when WaUd had just breathed his last, and his
brother SolaimAn had been saluted as Caliph. The
renowned HajjAj had preceded his sovereign, and had
expired five days before the end of Ramadan, a.e. 95.
MisA did not receive the reward due to his distinguished
services. Accused of peculation by the new CaUph, ho
was beaten ■with rods, and condemned to a fine of 100,000
pieces of gold ; and aU his goods were confiscated.
SolaimAn did not stop here : he caused 'Abd al-'Aziz, the
son of MiisA, to be put to death in Spain, and carried his
cruelty so far as to show his severed head to MiisA, asking
him whether he recognised it. He repUed that it ■was the
head of a man a thousand times superior to him who had
ordered his death. MiisA died soon after. As for Tirik,
there is no further mention of him after the beginning of
the reign of SolaimAn, and we must therefore suppose
that he retired into private life.
' Aecordisg ii> Fistera cjronicle.", Julisa'a hati«d of Eoderic uof
fro'ji the Iftttf r (t batiji^ dishonotu-wi hir. daTiyhVr.
574
MOHAMMEDANISM
[oUAYTADr.
BoiaimSu. 7. Sokimiii had neatly missed the throne. Walid, in
the very year of his death, wished to have hia son 'Abd
aX-'Aziz b. Walid chosen as his successor, and had offered
Solaimin a great sum of money to induce him to surrender
his rights to the Caliphate; but Solaimin obstinately
refused to do so. Walid went still further, and. sent
letters to the governors of all the provinces, calling on
them to make the people take the oath of allegiance to
his sc4i. None except Hajjij and Kotaiba b. Moslim
consented thus to set at nought the order of succession
established by "Abd al-Melik ; and Solaimiln succeeded
without difficulty at the death of his brother. We can
easily conceive the hatred felt by Solaimin for HajjAj,
and for aU that belonged to him, far cr near. Hajj.lj
himself escaped ■ by death ; but Solaimin poured out his
wrath on his family, and strove to undo all .that he had
done. First of all, Mohammed b. Kfcim, the conqueror
of India, who was coasin to HajjAj, was dismissed from
his post and outlawed. HajjAj had deprived Yazfd b.
Mohallab of the government of KliordsAn ; Solaimin
conferred on him that of 'IrAk. Kotiiba b. Moslim, on
learning the accession of Solaim&n, knew that his own
ruin was certain, and therefore anticipated tlie Caliph by
a revolt. But Solaimiln induced Kotaiba's troops to
desert by authorising them to return to their homes; and
when the illustrious general sought to carry his army with
him, a conspiracy was formed against him which ended in
his murder. Yazld b. Mohallab, who preferred KhorAsAn
to 'IrAlf, obtained permission to exchange. Immediately
on his return to KhorisAn he r- et on foot a series of new
expeditions against JorjAn and Tati^stAn, But the
inhabitants of KhorAsin, which he governed oppressively,
made complaints against him to the Caliph, accusing him
of practising extortions in order to obtain such a sum of
money as would enable him to rebel against his sovereign.
From that day SolaimAn determined to get rid of Yazld.
As, however, he was then dreaming of the conquest of
Constantinople, he thought it prudent to dissemble his
dissatisfaction for some time.
The Byzantine empire was disturbed by internal
troubles during the years A.D. 715-717. SolaimAn
resolved to take advantage of these in order to rid himself
for ever of the hereditary enemy, of Islam, and prepared a
formidable expedition. A fleet of eighteen hundrfed
vessels, equipped at Alexandria, sailed to the coasts of
Asia Minor, took on board the Moslem army, commanded
by Maslama, and transported it to Europe. This army
appeared under the walls of Constantinople, 15th August
717, five months after Leo III., the Isaurian, had ascended
the throne. Once more the Greek fire prevailed against
the Moslems. Tlieir fleet was destroyed by this terrible
engine of war ; the anny could obtain no fre-sh supply of
provisions, and suffered all the horrors of famine. Mean-
while the Caliph, who desired to be present in person at
the taking of Constantinople, had set out to join the
army. He fell ill at DAbik, not far from Aleppo, and died
there on the 22d of September in the same year, after
having nominated as his own successor his cousin, 'Omar
b. "Abd al-'Az(z, and as successor to the latter, Yazfd b.
,'Abd al-Melik, his own brother. In vain did the new
Caliph despatch from Egypt a fleet of four hundred ships
to carry arms and provisions to the army before Constanti-
nople ; thia fleet also was destroyed by the Greeks, and
the Moslem army was decimated by famine, and soon by
the plague as well. A hundred tliou.sand men perished
miserably under the walls of Constantinople, and Maslama
brought back to Asia Minor a mere handful of soldiers,
and that vath great difficulty.
Cn.kr II. 8. 'Omar b. 'Abd al-'Azlz, incensed at this disaster,
took. Vijs revenge on the Christians of his own states by
excluding them from all public employments, in spite o§
the great services they rendered there, . and by loading
them with imposts to such an extent that one public
functionary wrote thus to the Caliph : " If things continue
to go on in Egypt as at present, all the Christians will
become Moslems to escape taxation, and the State will
lose its revenue." To this the pious "Omar replied : " I
should look on the conversion of all the Christians as a
great piece of good-fortune ; for God sent his prophet to
act the part of an apostle, and not of a fax-gatherer."^ By
his religious intolerance, by the simplicity of his life, and
by his vigour in observing the precepts of his religion and
enforcing their observance, 'Omar has acquired in Moslea^
history the reputation of a saint. But the sanctity of a
prince does not ensure the greatness of a State ; and the
reign of 'Omar, as we shall see, was injurious rather than
advantageous to Islam. He alienated the provincial
governors by his severity ; and the family of 'AbbAs took
advantage of the general discontent to stir up the people
secretly, and thus -to prepare the way for the fall of the
dynasty.
It will be remembered that SolaimAn died before caiTj-
ing out his purpose of deposing Yazid b. Mohallab, the
governor of KhorAsAn. 'Omar II. took it on himself to
fulfil this design. He summoned Yazid to his presence,
and on his arrival at Damascus, threw him into prison,
and demanded the restitution of the money which he
believed him to have misappropriated. As Yazld alleged
that he could render no accoimt of it, the Caliph banii.htd
him to Dahlak, a small island in the Eed Sea, but soci
brought him back, and placed him in close ccnfinf.uient.
It was not till a.h. 101, when 'Omar II. was d3'ing, that
Yazfd succeeded in escaping and took refuge in "IrAk.
Mokhallad, the son of Yazld, whom his father, on quit-
ting KiorAsAn, had left there as his lieutenant, was also
summoned to Damascus, and the Caliph at first appointed
JarrAh b. 'AbdallAh governor of that province, but soon
after, on receiving complaints against him, replaced hiin
by "Abd al-EahmAn al-Koshairl, whom he desired to u.-^o
every effort for the conversion of the unbeliever.'-', rather
than to think of extending the jMoslem power by force
of arms. With so pacific a disposition, it is easy to
understand that the Caliph did not signalize his reign by
any conquest ; except a revolt of the KhArijites in "Iriti
which was suppressed by 'Maslama, his caliphate was not
distinguished by any warlike event. Its most noticeable
occurrence, as we have said above, was the commencemcnl
of the "AbbAsid movement.
The "AbbAsid family derived its name from 'AbbAs, wh> 'Abliig^.
was Mohammed's uncle on the father's side, and who, """!>•
during the Prophet's life, had enjoyed universal coiisidert ''"°"
tion among the Moslem.s. It was he who, at the death ci
the Prophet, had the charge of washing the corpse. The
first Caliphs, Abiibekr, "Omar, "OthmAn, and "Ali, showed
the utmost deference to 'AbbAs; and his eldest son
"AbdallAh had been united in the closest friendship with
Hosain, the unfortunate son of "AH. After the assassina-
tion of 'Ali, and the slaughter of Hos.iin, "AbdallAh had
retired to Mecca, and there brought up his numerous
family in hatred of the Omaj-yads. It was from his
youngest son "AH, born a.h. 40, that the "Abb.Asid dynasty
spnmg. Under the Caliph "Abd al-Mclik, this 'All was
living at Damascus ; but, on his marrying Labbaba, the
divorced wife of 'Abd al-Melik, the Caliph conceived a
great aversion for 'AH. WaUd, the son and successor of
'Abd al-Melik, inherited his father's prejudice.'!, subjected
'AH to every kind of insult, and drove liim from his court.
WaHd's successor, SolaimAn, gave him leave to return to
Damascus, but "AH, instead of availing himself of this
permission, preferred to retire to Homaima, a town situ.
CltAYTASS.]
M O H A .^t M E D A N I S M
575
ated in the south ot Syria, on the confines of Arabia. It
was in this retireinent that his son Mohammed conceived
the design of supplanting the Omajyad dynasty. We have
said that the first "Abbasids were closely united with the
family of 'All Mohammed b. 'All, the 'Abbisid, saw
clearly that it was only among the followers of "All that he
was Ukely to be able to form a party. To attain this
object, he formed the plan of making it believed that a
descendant of the Prophet's son-in-law had transmitted to
him his rights to the Caliphate. It will be remembejed
that Mohammed b. Hanaflya had come forward as a pre-
tender to the throno at the troublous period when Ibn
Zobair and 'Abd al-Melik were disputing the Caliphate.
According to the story of the 'Abbisids, Abii H4shim
'Abdalliih, the son ot Ibn Hanafiya, had gone to Homaima,
to the house of Mohammed b. "AJi, and had made on his
deathbed a legal transfer of his rights to Mohammed, by
appointing him his heir. Whatever may be the truth
respecting this transfer,^ Mohammed tha 'Abbisid spread
abroad the report of it, and chose especially for its pro-
pagation the provinces in which the family of 'AH had
the greatest number of adherents, 'Iralf and Khordsdn.
Emissaries sent by him into these two provinces, under
the caliphate of 'Omar II., began to stir up the people
in secret agsinst the reiguing house. 'Omar was probably
acquainted with these intrigues, but he had not time to
repress them, for ho died on the 20th or 25th of Bajab,
A.H. 101 (5th or 10th February 720), after a reign of
a1x)ut two years and a half.
Yaadn. 9. Y&zid, the sou of 'Abd al-Melik, ascended the
throne without resistance. His first care was to piirsue
Yazld b. Mohallal), who had escaped from his prison and
taken refuge in 'Irdlf. Besides reasons of state, Yazld IL
had personal reasons for ill-will to Yazid b. Mohallab,
One of the wives of the new Caliph, the same who gave
birth to that son of Yazld 11. who afterwards reigned
under the name of Walld 11., was niece to the celebrated
Hajjij, who, as it will be remembered, had hated and per-
secuted Yazld b. Mohallab. Aware of the alliance of the
new Caliph with the family of Hajjij, the son of Mohallab
had made every effort to escape as soon as he was informed
of the illness of 'Omar IL .; for he well knew that Yazld
IL would spare neither him nor his family. In fact,, the
Caliph sent ezpress orders to the prefect of "IrAlf to arrest
all the brothers and other members of the family of
Mohallab who were to be found ait Basra ; and this order
was immediately carried out. But Yazld b. Mohallab had
many partisans in 'Ir4k- He collected a small army, and
fought with such valour that in a short time he succeeded
in making himself master of Basra, where he had himself
proclaimed Caliph. The public treasury fell into his
hands, and he employed it in paying his troops and in
raising fresh ones, whom he sent on expeditions into
Khi\zistin or Ahwiz, Firsistin, Mokrin, and Sind. As
this revolt threatened to spread far and wide, Yazld IL
was obliged to have recourse for its suppression to the
celebrated Maslama. Early in a.h. 102, this illustrious
general took the field, and completely defeated Ibn
Mohallab near Basra, Y'azld fell in the battle, and his
brothers fled beyond the Indus, but were pursued and
slain by the lieutenants of Maslama.
This revolt suppressed, Yazld IL was able to give his
thoughts to the extension of the empire, an object which
had been so much neglected by his predecessor. Several
expeditions were directed against Farghina in Transoxiana,
against the Khazars in Armenia, and against the Greeks
in Asia Minor, but without any very decided results. In
' The 'Abbisid Caliph Ma'mun certainly did not believe in it, for be
thought it bis duty to restore the Caliphate to the family of 'All, by
apiwinting as hU successor 'Mi Ridi, a descendapt of the Caliph "Ali
Africa, serious troubles had been caused by tne appoint-'
ment as governor of a certain Yazld b. Abl Moslim, who
had been secretary to Hajj&j, and who followed the
example of his master's implacable harshness. The Ber-
bers rose in insurrection, slaughtered the unfortunate
governor, and chose in his place Mohammed b. Aus. The
CaUph at first ratified this choice, but soon after dismissed
Mohammed from his post, and replaced him by Bisbr b.
Safwin, who sent out an expedition against Sicily.
In Europe, the Arabs obtained at first some degree of
success. Under the orders of Samah, then governor of
Spain, they crossed the Pyrenees, and took possession of
Narbonne ; but, having been beaten at Toulouse, they had
to retrace their steps. It was the celebrated Abderams
('Abd al-Rahm4n) who effected their retreat.
Yazld n. died three years later of a lingering illness,
caused, it is said, by his grief for the death of a favourite
slave-girL At his accession, Yazld had designated as his
successors, in the first place his son Hishim, and in the
second his son Walld. HishAm ascended the throne
without opposition.
10. Hishim was a pious prince and an enemy of Uisbuu.
luxury ; as rigid in his religion as 'Omar II. To this
severity may in part be attributed the disturbances which
broke out in the provinces during his reign. The
governors were accustomed to remain loyal to the Caliphs
only when the latter did not exact from them too rigorous
an account. Hishim was, besides, very avaricious, a
fault highly calculated to make him odious to those about
him. Lastly, he favoured the Yemenites, and this
alienated from him the powerful party of the Kaisites.
All these circumstances emboldened the "Abbisids to carry
on actively their propaganda in 'Irik and KhorAsAn, and it'
succeeded beyond their hopes. The Kaisite tribes, offended
at seeing the Caliph bestow the best posts on Yemenites,
were ready to espouse with enthusiasm the cause of any
one whose aim was the overthrow of the Omayyads.
Eebellion had been smouldering in the provinces for
thirteen years ; it broke out at last at Cufa and in the
whole of 'IrAk, under chiefs called Moghlra and Bahliil ;
and when these insurgents had been chastised, others
sprung up in their place, 'Amr al-Yashkorl, Al-'Anazf,
and Al-Sakhtayinl The prefect of 'IrAk, KhAlid b.
'AbdallAh, was accused of favouring this revolt, was
degraded, and replaced by Yilsuf b. 'Omar, who threw
him into prison, where he remained for eighteen months.
This measure increased the discontent of the people of
'Irak, and a member of the family of "All, Zaid b. 'All,
collected round him a small body of partisans, and had
himself proclaimed CaUph, a.h. 122 (a.d. 739-740).
Unfortunately for Zaid, he had to do with the same Cufans Zajc" b>
whose fickleness had already been fatal to his family. In *'■•
the moment of danger he was deserted by his troops,
slain in an tmequal conflict, and his head sent to Damascus.
In KhordsAn also there were very serious disturbances.
In the year 106 (a.d. 724-725) there had already been
a revolt at Balkh, excited by the emissaries of the
"Abbisida. The following years brought with them fresh
troubles, which led to the dismissal of the governor of
EhorisAn, Asad, the brother of KhAlid b. "AbdaUAh, who
had been prefect of "Irik- Under the successors of Asad,
who were successively Ashras b. 'AbdallAh, Jonaid b.
'Abd al-Rahmin, and '.i^im b. 'AbdallAh, seditions broke
out in Transoxiana, which were repressed with great
difficulty ; and it was not until the year 1 20 that, by the
appointment of the brave and prudent Nasr b. Sayy4r
as governor of KhorisAn, peace was for a time restored'
to -that region. The 'Abbisid emissaries, nevertheless,,
secretly continued their propaganda.
In India, several provinces which had been converted
576
MOHAMMEDANISM
[OMAYYADS.
to Islam under the Caliphate of "Omar II. declared them-
selves independent ; and this led to the founding of
several strong cities for the purpose of controlling those
proviuces. Itjwas thus that the cities of Mahfiiza and
Mansiira had their origin.
In the north and north-west of the empire there were
no internal disorders, but the Moslems had much to do to
maintain themselves there against the Alans, the Turko-
mans, and the Khazars. The illustrious Maslama lost his
life in battle, and Merwin b. Mohammed, afterwards
Caliph, took his place as prefect of Armenia and Azer-
baijAn. He succeeded in imposing peace on the petty
princes of the Eastern Caucasus, and in consolidating the
Arab power in that quarter. The war against the Byzan-
tines lasted during the whole of HishAm's, reign. In Asia
Minor, the Moslems reoccupied Ccesarea, and laid siege to
Nicsa. Arab writers even declare that ConStantine, after-
wards Emperor of Constantinople, was made prisoner in
the year lU (a.d. 732-733), but the Byzantine authori-
ties make no mention of this fact. On the other hand,
they notice an important defeat of the Moslem arms in
A.D. 739. This defeat, which is acknowledged by the
Arab writers, -cost the life of their general, 'AbdallAh,
sumamed al-BatUl — "the hero" — whose prowess still
lives in the memory of the people of Asia Minor.
In Africa, several successive prefects were fully occupied
in repressing the constant insurrections of the Berbers.
In Spain, the attention of the Moslems was principally
turned to avenging their defeats beyond the Pyrenees.
As early as the second year of the reign of Hishdm,
'Anbasa, governor of Spain, crossed the Pyrenees, and
pushed on military operations vigorously. Carcassonne
and Nimes were taken. The death of 'Anbasa, in a.h.
107 (a.d. 725-726), put a stop to hostilities; but they
recommenced still more vigorously six years later. 'Abd
al-Rahmin (Abderame), the same who, under Yadd 11.,
had led back to Spain the remnants of the Moslem army,
crossed the mountains anew, and penetrated into Gascony
by the passage of Roncevaux. The Moslems beat the
Duke Eudes, gained possession of Bordeaux, and overran
the whole of Southern Gaul as far as the Loire. But in
A.H. 114 (a.d. 732) Charles Martel, whose aid the Duke
of Aquitaine had implored, succeeded in inflicting on "Abd
al-RalimAn so severe a defeat, near Poitiers, that the
Moslems were obliged to effect a hasty retreat, and to
return to Spain. Two years later the new governor of
Spain, "Olfba b. al-Hajj4j, re-entered Gaul, and pushed
forward expeditions as far as Burgundy and Dauphin^.
Charles Martel, with the help of the Lombards, again
drove back the Arabs as far as Narbonne. Thenceforth
the continual revolts of the Berbers in Africa on the one
side, and on the other the internal troubles which disturbed
Spain, and which led at a later period to its independence,
offered insurmountable obstacles to the ambition of the
Moslems, and prevented their resuming the offensivei.
Such was the state of the empire when Hishim died
on the 6th of Rabf 11. a.h. 125 (6th Feb. a.d.
743), after a reign of twenty years. He had not been
wanting in energy and ability. Yet under his reign the
'Moslem power declined rather than advanced, and signs
of the decay of the Omayyad dynasty began to show
themselves. The history of his four successors, Walfd II.,
Yazld III., Ibrihim, and ilerwin II., is but the history of
the fall of the Omayyads.
11. Walid II., the son of Yazid II., ascended the throne
without opposition at the death of HishAm ; but he soon
made himself so much hated and despised by his debauch-
cries and his irreligion that eysn the sons of HishAm and
of Walid I. plotted with the enemies of the Omayyads.
Yazld, one of the- sons of Walid I., went so far as to take
openly the title of Caliph, and to march against Damascus,
which Walid II. had quitted for fear of a pestilence which
was then raging there. This step was fatal to the Caliph.
The inhabitants of Damascus opened their gates to Yarld,
who took possession of the arsenals, and used the arms
they contained to equip new troops. Walid 11, on his
side, collected his adherents and marched against his rival.
The two armies met at a place called BakhrA, on the
confines of Syria and Arabia. Yazid had no difficulty in
overcoming his opponent, who was abandoned by his own
soldiers. Walid IL died fighting, having reigned little
more than a year, and his head was taken to Damascus,
and carried about the city at the end of a .spear. (JomAdI
n., A.H. 126, March-April 744.)
12. The death of Walid EI., far from appeasing theYaod
troubles of the State, put its unity in greater jeopardy than HI.
ever. The distant provinces escaped from the power of
the new Caliph. In Africa, 'Abd al-RahmAn b. Hablb
declared himself independent. In Spain, every emir
aspired to free himself from a suzerainty which appeared
to him only nominal In KhorisAu the 'AbbAsid emissaries
were more and more busy, acting in the name of IbrAhim
b. Mohammed, who had become the head of the family by
the death of his father, Mohammed b. 'All, Even in Syria
Yazld m. saw his authority disputed. Himself belong-
ing to the sect of Mo'tazilites, who rejected the doctrine
of predestination — a sect to which we shall have occasion
to recur in treating of the religious history of Islam —
he aroused all the orthodox against him. Besides this,
many of the Syrians, from a sudden change of feeling,
now desired to avenge the death of Walid IL The
inhabitants of Emesa revolted, and marched against
Damascus. They were beaten at a place called Thanlyat
al-'OkAb, or The Eagle's Pass, twelve miles from the
capital Palestine rose in its turn, and chose as its Caliph
anothef Yazid, cousin of the reigning prince. This revolt
also was suppressed. But a greater danger menaced
Yazld III. The Omayyad MerwAn b. Mohammed, who
was, as we have said, governor of Armenia and of Azer-
baijAn, also prepared to dispute the supreme power with
the Caliph of Damascus, and invaded Mesopotamia. Yazld
m, in his alarm, offered him the government of this last
province as the price of peace. MerwAn accepted these
conditions, but he would probably not have left his rival
long at rest, had not the latter dfed after a reign of only
six months.
13. Yazid nX left his brother IbrAhim as his successor. Ibrihlii.
At the news of Yazld's death, MerwAn collected a power-
ful army and entered Syria. Having beaten IbrAhim 's
generals one after the other and taken Emesa, he advanced
rapidly towards Damascus. SolaimAn b. HishAm tried to
oppose his march, but he was defeated at "Ain al-Jarr,
between Baalbec and Damascus, and the Caliph IbrAhim
took flight ; while SolaimAn, the son of HishAm, laid hands
on the public treasure, and then fled in turn. MerwAn
entered Damascus, and caused himself to bo proclaimed
Caliph. The reign of IbrAhim had lasted only two months.
IbrAhim himself soon acknowledged the new Caliph, and
submitted to his authority.
14. MerwAn IL was a man of energy, and might have Merwiii.
revived the strength of his dynasty, if the ferment in the ''■
east of the empire had been less strong. Unfortunately
for him, the "AbbAsid movement had never ceased to gain
ground in KhorAsAn, and the chief adherent of the family
of "AbbAs, Abu Moslim, was in no degree inferior to the
Caliph in energy and ability. This Abii Moslim, whose
origin is obscure and disputed, had been distinguished by
the "AbbAsid Mohammed b. 'Ali, the same who alleged that
he had been appointed heir to the claims of the family of
"AH to the supreme power. If wo may believe the legend,'
OKATTABS.]
MOHAMMEDANISM
577
Mohanuned had even foretold that die accession of his
family wonld take place t» the year of the a«,' through
the efforts of Abti Moslim, and that one of his three sons
would ascend the throne. These three sons were : Ibra-
him, "Abdallih, called Ab(i 'l-'Abb4s, and 'AbdallAh, called
Abii Ja'far. Whatever we may think of this prediction,
it is certain that under Iferwin EL Abii Moslim was the
principal emissary of the 'Abbisid Ibrihlm, and had been
able to form a vast conspiracy in KhorisAn, which broke
out in A.H. 128, at the very moment when it had been dis-
covered by Nasr b. SayyAr, the Omayyad governor of the
province. Even before this, Merwin II. had had to repress
disorders which had broken out in Syria, Palestine, and
Triik ; and the Caliph could new rely so little on Syria
that he had thought it necessary to quit Damascus, and to
fix his abode at Harrin, in Mesopotamia. On learning
the revolt of Abii Moslim, Merwin IL wrote to Kasr b.
Sayyir, directing h'"" to act with vigour against the
fomenters of sedition. It was easier to give such an order
than to execute it, for Abii Moslim was at the head of a
numerous army, absolutely devoted to ' the 'Abbisids.
Merwdn IL thought it necessary at the same time to
secure the perso» of the 'AbbSsid pretender Ibrdhim, who
was still living at Eomaima. Ibrihim was therefore
arrested, conveyed to Harrin, and thrown into prison.
He found means, however, of communicating with his
lieutenant Abii Moslim, and the latter, who had received
the most extensive powers from his chief, marched direct
upon Merv, the capital of Khor4s4n, and drove out the
governor Nasr. At the news of this the Caliph, no longer
able to restrain his anger, had his captive Ibrahim put
to death ; an execution which, at a later period, brought
upon the Omayyads the most terrible reprisals. The
brother of IbrAhlm, Abii 'l-'Abbis, surnamed SaffAh,
"The Sanguinary," on account of his cruelties, having
by Ibrihim'a death become chief of the 'Abbisids,
immediately quitted Homaima with all the members of
his family, and took refuge in Ehorisdn, that his pre-
sence there might sanction and encourage the insurrection.
Abii Moslim, now master of Khor4s4n by the capture of
Merv, had meanwhile sent an army against 'Irik, under
the orders of Kahtaba b. Shabib, who had beaten the
Omayyad army, commanded by Yazfd b. Hobaira,
governor of that province. In a.h. 132 Abii 'l-'AbbAs
arrived at Merv. After remaining there some time,
wailing for a favourable moment, he decided on openly
JU-SaffAli as.suini:ig the title of Caliph. He installed himself
jBjnmM ju {jjQ governor's palace, and thence went in state to
oiCsIipU. '^^ mosque, where he mounted the pulpit, and officiated
GZNEALOQICAL TABLE OF THE OUAVTADS.
Omayj-a.
in the capacity of successor of the Prophet. All those
present took the oath of allegiance to him, and Abii
VAbbis returned to the palace, over which the black
flag was flying, black being the distinctive colour of the
"Abbisids.^ But he did not remain long at Merv.
Committing the government of that city to his uncla
Diwiid, he went to review his army, and divided it
into several corps, which he directed against different
points. After this he went to Chaldjea, and there estab-
lished himself in a spot not far from Cufa, to which he
gave the name of Hishimlya, or the city of Hishim, the
ancestor of his own family and of that of the Prophet.
Another of his uncles, 'AbdallAh b. 'All, whom he had sent
on an expedition against the city of Shahrozur, took pos-
session of that place, and leaving Abii 'Aun 'Abd al-Melik b.
Yazld there as governor, rejoined his nephew and sovereign
at HAshimfya. Meanwhile the Omayyad Caliph had
marched against Shahroziir. Abil 'Aun went out to meet
him, and was joined by a strong reinforcement of cavalry
under 'Abdall4h b. 'ALL The 'Abbisids only numbered
forty-five thousand soldiers, but these were experienced
and resolute warriors. The Omayyad army, though much
more numerous, was ill commanded and devoid of spirit.
A battle ensued, and fortune fr.'oured the rebels. In
vain did MerwAn show himself everywhere ; his soldiers
gave way and repassed the Zdb in disorder, hurrying away
in their flight the unfortunate Merwin. (Jomidl EI. 11, A.B. Trinn.
132, 25th January 750.) This victory cost the Omayyads f '|"-
their empire. MerwAn attempted at first to take refuge ^^*
at Mosul ; but the inhabitants of that city having declared
for the enemy, the prince went to his capital Harr&n,
whence he was soon driven by the army of 'Abdallah b.
'All. From Harrin Merwin fled successively to Emesa,
to Damascus, to Palestine, and finally to Egypt. He was
pursued without intermission by Silih, brother of 'Abd-
allih b. 'All, who at last came up with him at Biislr,
on the frontiers of the Delta. Merwan took refuge in a
Coptic church ; but the 'Abbisids pursued him into the
building, and slew him at the foot of the altar. His head
was cut off and sent to Cufa, where the new Caliph then
was.
Thus perished in the East the dynasty of the house of
Oxa&yysL, which, having been founded by usur])ation, had
only maintained itself by shedding torrents of blood, and
was destined to perish in blood. We now enter upon
the history of the new dynasty, whose origin we have
described, and tinder which the jKiwer and glory of L-lam
reached their highest point.
Here we give the
Abii 'l-'is.
I
Hakam.
4.. Mebwan I.
I
Mohajnmed.
14. Mehwan n.
S. 'Abd al-Melie.
•Abd al-'Aziz.
I
8. 'OtUB IL
I
Harb.
Abii Sofyia._
1. Mo'awiya L
I
2. Yazid L
3. Mo'^wiTA IL
12. Yazid IIL 13. IbbXrIu.
9. YazId II.
11. Wali'd II.
' To landerstand this allnsion wo must know that Merwdn II. had
T«cAlved the Dickname of Bi:n&r, "the ass," on accout ortlia tempor-
Mnm and the strength of his constitution.
^ Historians are divided as to the date at which black became the
Abbisid colour. ' According to some, the first 'Abbisids wore a tob« | 'tida. Paris, 1837,
of black silk as early as at the battle cilled that of the Camel.
According to others, it was only after the murder of Ibiihini by Mer-
win that tho 'Abbisids adopted black as a sign of 'mourning. Se«
Quatremere, iftmoirea hisioriquca sur la dynastic da khali/ta Abbas-
XVL
-73
378
MOHAMMEDANISM
['AEBiaOS.
Sect. II. — The 'AbbXsids.
AW 1- From Uie death of Menvin may be reclfoned the
VAlibfsreal accession of the 'AbbAsid dynasty to the Calijfhate,
•l-S.ilTuL yvlih.'U thus returned to tlie hands of the grand-nejihews
of the Prophet. Abii 'l-"AbbAs, whose proper name was
'Abdalhlh, and who afterwards received the surname of
KafTcih, was, as has been said above, a man of energetic
will, who hc?itatcd at nothing to ensure the triumjih of
his dynasty. When he caused himself to bo proclaimed
Caliph at Cufa, one of his partisans, Abil Salama, who had
till then believed that Abii 'l-'AbbAs was working to restore
the posterity of "Ali to tljo throne, and not to gain posses-
sion of the empire for himself, hesitated to take the oath
of obedience to the new Caliph. Abii 'l-'Abbds immedi-
ately resolved on his. destruction, but fearing that Abu
Salama might have a secret understanding witli the con-
queror of KhorAsdn, he began by sending his own brother
Abu Ja'far into that province to sound Abil Moslira. The
latter loudly disclaimed any alliance with Abii Salama,
and, that no suspicion might rest upon him, he sent a
confidential agent to Cufa, and had Abii Salama assas-
sinated. Still further to prove his zeal for the house of
'Abb.ls, Abu Moslim also got rid of SolainiAn b. Kathir,
another ".^bbtisid emissary, whom he suspected of partiality
towards the family of 'All. On his side, Abil l-'Abb.is
caused '^\bdallah b. JIoMwiya, an adherent of 'All's family,
to be treueherously slaiu, though he had distinguished
himself iu the wars against Slerwdn. As for the Omayyads,
they were systematically followed up and put to death.
The new Caliph desired to exterminate that family, not
only for the sajte of revenge, but also that he might deprive
the Syrians of any prete.xt for fresh insurrections. In
fact, hardly had Abii 'l-'Abb,is been proclaimed Caliph at
C"fe) when the Omayyad governor of Kirmesrin, Abil
'i-i?iird b. Kauthar, notwithstanding that he had taken
the oath to the new sovereign, gave the signal for revolt
in the name of the Omayyads. Abii '1-' Abbas immediately
ordered his uncle 'Abdallah b. 'Ali, who had been made
governor of Palestine, to act with the utmost rigour
against all members of the Omayyad family on whom he
could lay hid hands. That he might let none of them
escape, 'AbdalUh pretended to grant an amnesty to
all Omayyads who should come in and acknowledge the
new Caliph, and even promised them the restitution of
all their property. Ninety members of that unfortunate
family allowed themselves to be entrapped by these
Epecious pron^ises, and 'AbdallAh, on pretence of sealing
the reconeiliation of the two parties, invited them to
a banquet. But when they were all collected, a body
of executioners rushed into the hall, and slew the
Omayj-ads with blows from whips and rods. A grandson
of HishAm, "Abd al-Rah.mAn b. Mo'iwiya, who had taken
refuge in Africa, alone escaped this massacre. It was he
who, at a later date, founded in Spain the Omaj-j'ad
dynasty of Cordova. The cruelty of the "AbbAsids excited
Ik feeling of horror in the whole of Syria, and the revolt
.soon became general. Abii '1-Ward b. Kauthar found
liimself at the head of forty thousand men, and pitched
his camp at Marj al-Akhram, a plain near Kinnesrin.
'J'ho revolt spread even to Mesoijotaniia and 'Ir.Al;. One
of JlerwAn's former generals, IsliAlf b. Moslim, laid siege
to llarrin, while Yazid b. Ilobaira, formerly governor of
'IrAlj, raised an insurrection at WAsit. In KhorAsAn also,
as many as thirty thousand malcontents took up arms
against Abil Moslim. Notwithstanumg this formidable
display of force, the 'AbbAsids remained conquerors. In
Syria, 'AbdallAh b. 'All beat Abii 'l-Ward at Marj al-
Akhram. Abii Ja'far, brother of the CaliiJi, compelled
laliAk b. Moslim and Yazid b. Ilobaira in Euccession to
submit. Lastly, Abii Moslim quieted the riaing La
KhorAiAn. Mosul a!so attempted an insurrection, but
YahyA, a brother of the Caliph, quenched the revolt ia
streams of blood. All the jirovinces being thus reduced
to peace, the new Caliph distributed them among the
principal members of his family and his best generals.
To his brother Abii Ja'far he gave a jiart of Mesoix)tamia,
jViicrbaijAn, and Armenia ; to his uncle "AbdallAh b. 'Ali,
Syria ; to his uncle DA-\nid, Arabia, KijAz, YamAma,
and Yemen ; to his cousin 'IsA b. Miisi, the province of
Cufa. Abii iloslim continued in posses.sion of the govern-
ment of KhorAsAn, Transoxiana, and a part of FAr-iistAn,
Eg)pt was entrusted to Abii 'Aun. Another uncle of the
Caliph, SolaimAn b. "AH, received the government of
Ba.sra, with Bahrain and 'Oman. I.astly, the province of
" Mosul was taken from the cnrel Yahya, and granted to
one of the rmcles of Abii 'l-'AbbAs, IsmA'll b. 'ALf, who
received besides .the government of AhwAz. In Sind, the
Omayyad governor had succeeded in maintaining himself,
but was defeated by an army sent again.st hiiii under
MiisA b. Ka'b, and the black standard of the 'AbbAsids
was raised over the city of Man.silra. If wo omit Africa
and Spain in describing this division of the provinces of
the empire, it is because the 'AbbAsids never gained any
real footing in Sjjain, while Africa remained in only
nominal subjection to the new dynasty.
Abil 'l-'Abbas, after having definitively established his
power, left the iovra of HAshimiya and fixed his residence
at AnbAr, where he died on the 13th of Dhii '1-Hijja, A.H,
136 (9th June 754).
_ 2. Abii 'l-"Abb.As had designated as his successors, first Atii J»
Abii Ja'far, and after him bus cousin 'IsA b. Miisi. At "f" »\-
the moment of the death of Abii 'l-'Abb;ts, Abii Ja'far, ^'^S"'-
who then assumed tlie title of Al-Mansiir, "the Victo-
riou.s," was not in 'Irak. He had undertaken the leader-
ship of the jjilgrims who had started on the journey to
Jlecca, and among whom figured the celebrated Abii
Moslim. 'AbdallAh b. 'Ali, uncle of Abil 'l-'AbbA-s, dis-
satisfied at having been excluded from the succession,
took advantage of this absence to revolt. Having raised
an army and proclaimed himself Cahph, he marched
against HarrAn and laid siege to it. On receiving thii
news, Abii Ja'far hastened to return to AnbAr in company
with Abii Moslim, whom he placed at the head of h'-i
troops, and sent against the rebel At the approach
of Abii Jloslini, 'AbdallAh, who had among his troojis a
body of seventeen thousand men of KhorAsAn, fearing
that they might declare for Abii Moslira, had them all
slaughtered, as the historians assert, by his Syrians, and
then hastened to meet his enemy. The two armies met
at Nisibis, and, after a number of skirmishes, a decisive
engagement took place on the 7th of JomAdi II., a.h. 137
(28th November 754). 'AbdallAh was defeated and com-
pelled to submit to Al-Man.silr, who spared his life. Tlie
new and brilliant service thus rendered by Abil Jloslim to
his sovereign ought to have placed him even higher in the
favour of Mansiir than he already stood. On the contrary,
it was the cause of his ruin. The Caliph wished to com-
mit the task of maintaining order in Syria to Ab« Moslim ;
but the latter refused to give up his government of
KhorAsAn, where he enjoyed an extraordinary reputation,
and possessed numerous adherents, and, instead of obeying
the order of the Caliph, directed his march towards the
East. Thenceforth Mansiir loi.l.cJ on him only as a
dangerous rebel, and sought f.T means of getting rid of
him. On pretence of conferring with 'I'l,! on business of
state, he induced him to come to Mail, in (the ancient
Ctesiphon), caused him to be jiut to death bv his i^ni.irds,
ard ordered his body to be tl.nnvn into the 'i !.;ris. Thus
miserably perished the real '..under of ti;c 'AbbAsiJ
-ABBisnNS.]
MOHAMMEDANISM
679
dynasty, after having accomplished his work, which, as
the historians assert, cost the lives of more than 600,000
men. Notwithstanding the defeat of 'Abdallih b. 'AH
and the murder of Abii Moslim, the spirit of rebellion was
not yet broken. Eisings took place in Mesopotamia and
to a still greater extent in Khorisin ; and the Caliph's
troops were repeatedly beaten by the rebels ; but order
was at last re-established by Mansiir's generals, by Khdzim
b. Khozaima in Mesopotamia, and by Mohammed b. al-
Ash'ath in Khorisdn.
About the same time Africa and Spain escaped from
the dominion of the Eastern Calii)hate ; the former for a
season, the latter permanently. The cause of the revolt
of Africa was as follows : As soon as Mansur ascended the
throne, he wrote to 'Abd al-Rahmin, announcing the
death of Abii 'l-"Abb4s, and requiring him to take the
oath of allegiance. 'Abd al-Rahm4n sent in his adhesion
to the new Caliph, and added a few presents of little value.
The Caliph was so much dissatisfied that he replied by a
threatening letter which excited the anger of 'Abd al-
Ralimdn. Ho called the people together at the hour of
prayer, mounted the pulpit, publicly cursed Mansiir, and
then declared his deposition from the CaKphate. He next
caused a circular letter to be -WTitten, commanding all
Maghrebins to refuse obedience to the Caliph ; and this
letter was circulated and read from the pulpit throughout
the whole extent of the Maghrib (the West). A brother of
'Abd al-Rahm4n, llyds, saw in this revolt an opportunity of
obtaining the government of Africa for himself. Seconded
by many of the inhabitants of Kairawin, who had
remained faithful to the cause of the 'Abb4sids, he attacked
his brother, slew him, and proclaimed himself govenior in
his stead. This revolution in favour of the 'AbbAsids was,
however, of no long duration. Habib, the eldest son of
'Abd al-Rahmdn, had fled on the night of his father's
murder, and Ilyds caused him to be pursued, with the
object of transporting him to Andalusia. Habib was
captured, but the vessel which was to convey him to Spain
having been detained in port by stress of weather, the
partisans of independence took arms, rescued Habfb, and
prepared to resist Ilyis, who was marching against (hem
at the head of an army. Under these circximstances a
fortunate idea occurred to Habfb. He challenged his
uncle Ilyis to single combat. Ilyis hesitated, but his
own soldiers compelled him to accept the challenge. He
measured arms with Habib, and was laid prostrate by
him with a thrust of his lance. The party of independ-
ence thus triumphed, and several years elapsed before the
The Agh- 'Abbisid general, Al-Aghlab, was able to enter KairawAn,
labites in and regain possession of Africa in the name of the Eastern
^^'^*- Caliph. From this time forward, it must bo added, Africa
only nominally belonged to the 'Abbdsids ; for, under the
Caliphate of Hdriin al-Rashfd, Ibrdhim, the son of Al-
Aghlab, who was invested with the government of Africa,
founded in that province a distinct dynasty, that of the
Aghlabites.
Spaiji.<.h Coincidently with the revolt in Africa, the inacpendent
Caliph- Caliphate of the Western Omayyads was founded in Spain.
*'*'' The long dissensions which had preceded the fall of that
dynasty in the East, had already prepared the way for the
independence of a province so distant from the centre
of the empire. Every petty emir there tried to seize
sovereign power for himself, and the people groaned under
the consequent anarchy. ■ Weary of these commotions, the
Arabs of Spain at last came to an understanding among
themselves for the election of a Caliph, and their choice fell
nppn the last survivor of the Omayyads, 'Abd al-Rahmdn
b. Mo'dwiya, • grandson of the Caliph Hishdm. This
prince was wandering in the deserts of Africa, pursued
by his' implacable enemies, but eserjofihere protected and.
concealed by the desert tribes, who pitied his misfortunes
and respected his illustrious origin. A deputation from
Andalusia sought hiih'out in Africa, and offered him the
Caliphate of Spain, which he accepted with Joy. On 25tb
September, A.D. 755, "Abd al-Bahmdn landed in the Iberian
Peninsula, where he was universally welcomed, and
speedily founded at Cordova the Western Omayyad Caliph-
ate, with which this history has no further concern.
While Manstir was thus losing ^rica and Spain, he was
trying to take from the Greeks the city of Malatiya,
which, from the importance of its situation, was looked
on as the key of Asia Minor. In A.n. 139-140 (a.d. V56-
757), a Moslem army of 70,000 men invested the place,
and, after a vigorous siege, Malatiya was taken by
assault. After this success the Moslems marched through
Cilicia, entered Patiphylia, and cut to pieces a Greek
am\y on the banks of the Melas. The Greeks asked and
obtained a seven years' truce, which Manstir was the more
disposed to grant because new and very serious troubles
had been stirred up in his empire by certain sectaries
of KhordsAn, called Rdwandfs. These Edwandis, like
many other Persian sectaries, admitted a number of
dogmas completely foreign to Islam, such as the trans-
migration of souls and the incarnation of the Deity as a
man. They believed, for instance, as historians assure
us, that divine honours ought to be paid to the Caliph
JIansur. They had their name from Rdwand, a city
near Isfahdn, where the sect originated. A great number
of these sectaries had repaired to Hdshimfya, the residence
of the Caliph, and there persisted in marching in pro-
cession round his palace, as if it had been the Ka'ba.
Mansiir, refusing to receive this impious homage, caused
the principal chiefs of the sect to be seized and throwa
into prison. The Edwandis immediately rose in revolt,
broke open the prson doors, rescued their chiefs, and
pushed their audai;ity so far as to besiege the Caliph
in his own palace. Very fortunately for Mansiir, tlie
populace declared against the Rdwandfs and massacred
them ; but from that time forward he took a dislike to
tho city of Hdshimfya, and resolved to choose another
residence. He had at first thought of fixing his place of
abode at Cufa ; but he remembciycd the fickle character of
the inhabitants, and decided on founding an entirely new
city on the banks of the Tigris. His choice fell upon
a spot near tho ancient Ctesiphon, the capital of the I'ouiia:.-
Sassanids, called Baghddd. There he himself laid thet'""."'
first stone of the city which was to be the centre of thu ^S"
civilised world as long as the Caliphate lasted. A revolt,
however, of some importance soon called Mansiir's atten-
tion from the building of Baghddd. The descendants of
"All, who had had reason to think that the "Abbdsids
were laboiu-ing for their advancement, were now cruelly un-
deceived. In A.H. 145 (A.D. 762-763), Mohammed Mahdi,
great-grandson of Hosain, and surnamed Al-Nafs al-Zakiya
(" the pure soul "), collected a large number of adherents
at Medina, and had himself proclaimed Caliph. The
governor- of Cufa, 'tsd b. Miisd, received orders to march
against him, and entered Arabia. The partisans of 'All
were defeated, and Mohammed Mahdi fell in battle. But
meanv/hile his brother Ibrdhfm had gone to Basra, and
had there succeeded in exciting a revolt, in presence of
which the 'Abbdsid governor had been obliged to capitu-
. late. The adherents of 'AU, emboldened by this success,
spread themselves over "Irdlf, and obtained possession of
several places, among which was the city of Wdsit.
Ibrdhim was already advancing towards Cufa, at the
head of a strong army, when "tsd b. Miisd, who had been
hastily recalled from Arabia, threw himself in his way.
A terrible conflict took place. ,, At last Ibrdhfm fell,
4)icrced.-by an arrow, andt in spite pi the desperate. efforli
580
MOHAMMEDANISM
['ABBASIDa.
of Ilia followeis, hia body remained in tho hands ot the
Enemy. The partisans of 'AH then dispersed, and never
eigain ventured to have recourse to arms.
The Caliph was highly delighted when he heard of the
decisive victory gained by 'Is4, bat, far from rewarding
his valiant cousin, he tried to compel him to renounce his
right of succession to the Caliphate, with the view of
EuV«tituting as heir-presumptive his own son Mohammed.
IsA at first energetically refused to abandon his rights -
but Mansiir did not hesitate at a shameless deception, and
produced false witnesses, who swore that 'IsA had waived
hia claim in favour of Mohammed b. Manstir. However
unwillingly, 'IsA was obliged to yield his priority to
iMohammed, but it was understood that, in case of the
death of the latter, the succession should return to 'Isi,
One of the false witnesses was, it is asserted, Khilid b.
Barmak, the lieAd of that celebrated Persian family the
Barmecides, which played so important a part in the reign
of Hardn al-Rashld. To this IChilid, Manstir had
entrusted the elevated post of minister of finance.
In A.H. 158 (A.D. 774-775), Mansilr, feeling the decline
of his powers, resolved to undertake for the last time the
pilgrimage to Mecca. At the last station on the route he
had a fall from his horse, and died at the gate of the Holy
City. He was nearly seventy years of age, and had
leigncd for twenty-two years. He was buried at Mecca.
3. Mohammed b. Mansilr was at Baghdid when ho
received the news of his father's death, and hastenea to
have himself proclaimed Cahph. He then took the title
t>{ Mahdl (" the well-directed "). To make his accession
Tvelcome to his subjects, he began by granting an amnesty
to a great number of persons who had incurred the anger
of Mansiir, and had been thrown into prison. Among
these was a certain Diwiid b. Yalfiib, whom Mahdf after-
wards made his prime miuistei'. But, on the other hand,
Mahdl did not choose to confirm in their posts the pro-
vincial governors in whom his father had placed confidence ;
he supplied their places by creatures of his own. These
ijhanges displeased the people of Khorisin, who revolted
under the leadership of a certain Yilsuf b. Ibrihlm, sut-
nanied Al-Barm. Mahdl Sent against him hia general
Ynzld b. Mazyad, who, after a desperate struggle, defeated
Tiisuf, took him prisoner, and brought him in triumph to
Bagtidid, where he was put to the torture and crucified.
Mahdl had been scarcely a year on the throne, when he
jrcaolved to accomplish the pilgrimage to Mecca, and at the
£a;ne time to visit the tomb of his father. Leaving his
eldest son Musi as governor of Baghdid, he set off,
accompanied by his second son Hiriin and a numerous
suite. The chroniclers relate that the Caliph had ordered
.* great number of camels to beladen with snow, and that
he reached Mecca without having exhausted this store.
(Immediately on his arrival in the Holy City, he applied
'liimself, at the request of the inhabitants, to the renewal
of the veils which covered the exterior walls of the Ka'ba.
Pur a very long time these veils had been placed one over
another, no care having been taken to remove the old
covering when a new one was put on ; bo that the'accumu-
lated weight caused uneasiness respecting the stability of
the walls. Mahdi caused the temple to be entirely stripped,
and covered the walls again with a single veil of great
richness. On this occasion Cp distributed considerable
largesses among the Meicans. From Mecca, Alahdl wont
to .Medina, vvnere he caused iho mosque la be enlarged.
0 luring his stay in that city Se formed himself a guard
of honour, composed of five hundred descendants of the
Ana.ir,' to wnom he assigned lands in Irik to be held in
^ The first citlzenj of Medina irho embraced U\uti were callod Anit&r ;
tee above, p. 664.
fief. Struck by the difficulties of every kind which had
to be encountered by poor pilgrims who desired to repair
to Mecca from Baghdid and its neighbourhood, ho resolved
to come to their help. His first care was to have the road
from Baghdad to Mecca laid out, and its divisions marked
by milestones. He next ordered the construction at every
stage of a kind of inn, where the poorer travellers might
find shelter and food. He also saw to having new wella
dug and cisterns built along the whole route
Whilst he was devoting himself to these pions'iaooura^
he was menaced by a dangerous revolt in KhorAsin. Ita
leader was a sectary called Hakim, surnamed Al-Mo^anna;
or the Veiled One, because he never appeared in public
without having his face eovered with a mask. Al-
Mokanna' hoped to gather a great number of adherents
around him, and to govern the province as absolutely as
Abii Moslim had formerly done. His religious teaching
consisted in the assertion that God had several times
become incarnate among men, and that his last incarna-
tion was Molfanna' himself. Many Persians were seduced
by his words, and still more by the hope of phmdering
the property of the Moslems, which Mokanna' promised
to give up to them. The governor of Khorisin and
several oth:r generals who marched against these sectaries
were defeated ; but at last the Caliph charged a skilful
captain, Sa'id al-Harashl, with the direction of operations,
and Sa'id, having compelled the impostor to throw him-
self into the city of Kash, soon reduced him to a choice
between surrender and death. Molfanna' preferred the
latter alternative, and took poison.
IhesB disturbances did not suffice to turn Mahdfs
tfioughta from the hereditary enemy of the Caliphate.
Every summer be sent expeditions into Asia Jlinor
against the Greeks ; but these were not successful, and
the Caliph decided on leading hia army in persoa Having
levied in Khorisin a large number of those mountaineers
who had always distinguished themselves by their valour,
he assembled his army in the plains of BaradAn, on the
banks of the Tigris, and commenced his march A.H. 163,
taking with him his second son Hiriin, and leaving his
eldest son MilsA as governor of Baghdid. The latter waa
also designated as his successor in the Caliphate, 'tsi b.
Miisi having definitively renounced the throne. Mahdl
traversed Mesopotamia and Syria, entered Cilicia, and
established himself on the banks of the Jaihdn (Pyramusi.
Thence he despatched an expeditionary force, at the head
of which hia son HAriin waa nominally placed. In reality,
that prince being too young to direct military operations,
the chief command was exercised by hia tutor, the
Barmecide Yahyi b. Kh.^lid. Hariin took the fortresa oi
Samilii after a siege of thirty-eight days. In consequence
of this feat of arms, Mahdl made Hiriin governor oi
Azcrbaijin and Ajmenia. Two years later war broke
out afresh between the Moslems and the Greeks. jLco
IV., Emperor of Constantinople, had recently died, leaving
the crown to Constantino Porphyrogenitas. This prince
was then only ten years old, and would have been incap-
able of governing. His mother Irene took the regency oi)
herself. By her orders an army of 90,000 men, nndei
the cogimand of Michael Lachonodracon, entered Asii
Minor. The Moslems, on their side, invaded Cilicia
under the orders of 'Abd al-Kabir, but were defeatecl by
the Greeks. Mahdl then recalled hia son Hinin, and
enjoined on him to avenge the failure of the arms ot
Islam. Hinin as-sembled an army of nearly 100,000
men, \nd conceived the project of carrying the w^r to the
very gates of Constantinople. Tho patrician Nicetaa,
who sought to oppose nis marcb, was defeated by Hiriin'a
general, Yazld b. Mazyad, and forced to take refuge at
Nicomedia. Hiriin marched through Asia Minor, tnd.
'abbAsids.]
MOHAMMEDANISM
581
pitched his camp en the shores of the Bosphorus. Irene
took alarm, sued for peace, and obtained it, but on
homiliating conditions. This brilliant success increased
Mahdi's affection for Hin^ to suoh an extent that he
resolved, a few years later, to declare him bis successor
(instead of M\i3^ It was necessary first to obtain from
iiiiii. & renunciation of his rights ; and for this purpose
his father recalled him from JorjAn, where he was then
engaged on an expedition against the rebels of TabaristAh.
Misd, who had had information of his father's intentions,
refused to obey this order. Mahdl determined to march
in person against his rebellious son (a.h. 169), and set
out, accompanied by HAriln. But, after his arrival at
MisabadhAn, a place in Persian IrA^ or Jabal, the Caliph
died suddenly, at the age of only forty-three. There are two
versions of the cause of his death : some attribute it to
an accident met with in hunting ; others believe him to
have been poisoned. If this was really the case, although
we have no proofs against Miisi, we may reasonably sus-
' pect him of having been privy tj the sudden death o^ his
father.
i. Mahdi having died before he could carry out his
plan for assuring the throne to HAniii, the succession natur-
ally fell to MiisA, and he was proclaimed CMiph at Baghdid
in the year of his father's death. He took the title of
H4df (He who directs). HArtlin made no opposition to the,
accession of his brother, and the army which had accom-
panied Mahdi returned peacefully from Jabal to Baghddd.
The accession of a new Caliph doubtless appeared to the
partisans of the house of 'All a favourable opportunity for
a rising. Hosain b. 'All, a descendant of that Hasan who
had formerly renounced his pretensions to th« Caliphate
through fear of Mo'dwiya L, raised an insurrection at
Medina with the support of numerous adherents, and had
himself proclaimed Caliph.' But having pifortunately
conceived the idea of going on pilgrimage to Mecca, ho
was attacked at Fakh by a party of 'Abbisids, and
perished in the combat. His cousin Idrls b. 'AbdaUAh
Buccceded in escaping and fled to Egypt, whence he passed
into Morocco ; and there, at a later period, hie son
founded the Idrisite dynasty.
HAdl, as may 1)6 supposed, "had never been able to forget
that he had narrowly escaped being supplanted by his
brother. He formed a plan for excluding HAnin from the
Caliphate, and transmitting the succession to his own son
Ja'far. He neglected no possible means of attaining this
object, and obtained the assent of his ministers, and of the
principal chiefs of his army, who took the oath of allegiance
to Ja'far. Only Yahyi b. KhAlid the Barmecide, HAnin's
former tutor, absolutely refused to betray the interests of
Lis pupiL. In a discussion which took place between him
and the Caliph on this subject, YahyA showed such firm-
ness and boldness that HAdl resolved on his death, and
Hai-thama b. A^an, one of the bravest generals of the
empire, had already received the order to go and take his
head, when the Caliph died suddenly. One of those
terrible domestic dramas had been acted of which so many
were afterwards seen in the palace of the Caliphs. . The
mother of HAdl and HAnin'was KhaizorAn, a haughty and
intriguing woman, whose aim it was to get the direction
of afiairs into her own hands, leaving HAdl only the shadow
of power. Her influence over all matters of government
was BO well understood that her door was beset all day
by a crowd of petitioners, who neglected the Caliph and
preferred to address their requests to her. HAdl soon
became indignant at the subordinate part which .his
mother \\'ished him to play, and after a dispute on the
matter, ho attempted to poison her. KhaizorAn, hoping
to find a more submissive instrument of her will in her
second son. and wishinc to protect herself against fresh I
attempts at murder, caused HAdl to be taken unawares
and smothered with cushions by two young slave.s whom
she had presented to him. (Babl' L, a.ii. 170, Sept.
A.D. 786.) '^
5. We have now reached &o most celebrated namendtr.ii
among the Arabian Caliphs, celebrated not only in the-'i^a'
East, but in the West as well, where the stories of the '*'''''•
Thousand and One Nights have made us familiar with
that world which the narrators have been pleased to
represent to us in such brilliant colours.
On the unexpected death of HAdl, the generals and
ministers who had declared against HAriin, perceiving that
popular favour did not incline to the son of the lata
Caliph, hastened to rally round the son of KhaizorAn ;
and HAriin, suruamed Al-Rashid (The Upright), ascended
the throne without opposition. His first act was to choose
as prime minister his former tutor, the faithful YahyA b.
KhAUd, and to confide important posts to the two sons of
YahyA, Fadl and Ja'far, the former of whom was also his
own foster-brother. The Barmecide family were endued
in the highest degree with those qualities of generosity
and liberality which the Arabs prized so highly. Thus
the chroniclers are never wearied in their praises of the
Barmecides. Loaded with all the hardens of government,
YahyA brought the most distinguished abUitios to the
exercise of his ofiice. Ho put the frontiers in a state of
defence, and supplied all that was wanting for their
security. He filled the public treasiu-y, and carried tho
splendour of the throne to the highest point. The
foUovring anecdote will show what an amount of earnest
afltection the Barmecide family succeeded in winning : —
After HaxAn, as we shall relato farther on, had ruined tho
Barmecides of whose influence he was jealous, lie forbade the poets*
to compose elegies on tho disgrace of the family, and commanded
that all who disobeyed this order should be puniahed. One day,
as one of the soldiers of the Caliph's guard was passing near a
mined building, he perceived a man holding a paper in his hand,
and reciting aloud, and with many te.ira, a lament over tho ruin of
tho palace of the Barmecides, 'fhe soldier arrested the man and
led nim to the pakce of the Caliph, who ordered the- culprit to be
brought before him, and asked him why he had infringed his
orders. "Prince," replied the man, *'lct mo relate my history to
thee ; when thou hast heard it, do with me as thou wilt. I was aa
inferior clerk tmder YahyA b. Khulid. He said to me one day :
* Thou must invite me to thy house.' ' My lord,* I replied, * 1 am
quite unworthy of snch an honour, and my house i« not fit tO'
receive thee." ' No, ' sdd Yahyd, " thou must absolutely do what I
require of thee.' ' In that case,' answered I, * grant me some littl&
delay that 1 may moke suitable arrangements.' Yahya granted me
some months. As soon as 1 informed him that 1 was ready, he
repaired to my abode, accompanied by his two sons, Fadl and
Ja'far, and by some of his most int'jiale friends. Scarcely had he
dismounted from his horse when *e begged mo to give him some-
thiag to eat. I offered him com roasted chickeNS. 'ft'hen he had
eaten his fill, he went over the ^Mlolo of my house, and having seen
it all, he asked me to show him the buildings attached to it ' My
lord,' said I, 'thou hast seen evijiything. ' 'No,' said he, 'thou
hast another house.' In vain I assured him that 1 had but one ;
he persisted in his a.*;sertion, and, sending for a mason, ordered
him to make an ofiening in tho walL ' My lord,' said I, ' may I
venture thus to mako my way into my neighbour's house ? ' * It
matters not,' replied he. 'When a doorway had been opened, he
passed through it, followed by his two sons, ajid I went after him.
V^o entered a delightful garden, well planted and watered by
fountains. In this garden stood a beautiful house n-ith pavilion*
adorned with furniture and carpets, and filled with slaves of both.
BCS03, all of perfect beauty. 'Ail thLs is thine,' said Yahya to me.
I kissed his hands and poured out my thanks to him ; and then I
learned that on the very day when he had spoken to me of iiivitinff
him he had bought tho land adjoining to my house, and had had
it laid out for mo without my ever suspecting it. I had certainly
noticed that building was going on, but I was far from ima^ning
that all this was intended for mo. Yahya next addressed himself
to Ja'far and said : ' Here are certainly ^ house and servants, but
who will provide for their support?' 'I,' replied Ja'far, 'will
give him a farm and its de]>endcncie8, and will send him the deed
of gift.' 'Very well,' continued YaliyA ; 'but how in he to livd
until he shall receive the revenue of his property V 'I owe bim ft
thousand pieces of gold,' eoid Fadl, ' and I will send them to hi*
582
M O H A M M P] D A N I S M
['aBBA3U)5.
honac' Tl:ark3 to ttcso magnilicont gifts, I afterwarda raiacd
ffreiit wea'th, — wealth which I still enjoy. SIdco that day, I have
nerer lost any oppoitinity of singing the praises of t!mt noblo
fanjily. And now. Prince, slay me if thou wilt ; I am ready to
die." Hariin, affected by this, tale, let tho man depart, and in
future forbade no man to weep for the tragical end of the sons cf
Barmak. {El-l''ac!iri, ed. Ahlwardt, p. 237.)
Although (he administration of H.'iriin's states ■wa.n com-
mitted to skilful hands, yet the first years of liis long
reign were not free from troubles. Towards tho jear 176
(a.d. 792-793), a member of the house of "All, named
Yahyi b. 'Abdallih, -n'ho had taken refuge at Dailam on
the Bhores of the Caspian Sea, succeeded in forming a
powerful party, and publicly announced his pretensions
to tho Caliphate. Hariiu immediately sent an army
of 50,000 men against the rebel, under the command of
Fadl. Pieluctant, however, to fight against a descendant
of the Prophet, Fadl first attempted to induce him to sub-
icit, by promising him safety for his life and a brilliant
position at the court of Baghdid. YahyA accepted these
conditions, but he required that tho Caliph should send
him letters of pardon countersigned by tho highest legal
a-utcorities and the principal personages of the empire.
E4nin consented to do so, and Yahyi, furnished with the
Caliph's safe-conduct, repaired to BaghdAd, where he met
wi<i a s;ilendid reception. At "ihe <ind of some months,
iswever, he was calummousfy accused of conspiracy, and
the Caliph, seizing this opportunity of ridding himself of
•, rival who might prove dangerous, threw him into prison,
where ho was soon after put to death. Dreading fresh
insurrections, Hirun thought it well to oecure the person
«f another descendant of 'All, Musi b. Ja'far, who was
resident at Medina, where he enjoyed the highest consider-
ation. The unfortunate man was seat to Baghdid, and
there died by poison.
Meanwhile Hiriin did not forget tho hereditary enemy
against whom he had already fought. Under his reign
all the ftrong places of Syria were formed into a special
province, which received the name of "Awdsim. The
charge of fortifying the city of Tarsus v/as committed to
Faraj, tho chief of the Turkish soldiers, whom the Caliphs
were beginning to employ, and who were at a later period
to become their masters. The ancient Anazarbrj was
rebuilt, and garrisoned with -a mUitary colony from
IChorisAn. Thanks to these measures, tho Moslem armies
were able to advance boldly into Asia Minor. Ishi^: b.
Solaimdn c'-.ered Phrygia and defeated the Greek gover-
nor of t'.at province. A Moslem fleet destroyed that of
the Greeks in tho Gulf of SataUa. HArun in person
invaded Asia Minor in the year 181 (a.d. 797-793), and
■during the following years his generals gained continual
victories over the Eyiantines, so that Irene was compellod
to sue for peace. An attack by the Khazars called tho
Caliph's attention from his successes in Asia INIinor. That
peoplo had made an irruption into Armenia, and their
attack had been so sudden that the I.Ioslcnis wore unable
to defend themselves, and a hundred thousand of them
had been reduced to captivity. Two valiant generals,
Khozaima b. Kh.'izim and Yazid b. Mazyad, marched
against the Khazars and drove them out of Armenia.
" In tho midst of the cares of war, HArun did not forget
his religious duties, and few years passed without his
making the pilgrimage. In one of these pilgrimages, a.h.
18G (a.d. 802), he was accompanied by his t%vo eldest
son;:, Mohammed and 'AbdallAh, and having determined
to fix the order of succession in so formal a manner as to
take away all pretext for future contentions, he executed
a deed by v/hich he appointed Mohammed his immediate
heir ; after him 'AbdallAh, and 'after 'AbdallAh a third of
his sons, named KAsim. Mohammed received the suraamo
of Al-Amin (The Stu-e), 'AbdallAh that of Al-Ma'miin (Ha
in whom men trust), and KAsim that of Mo'tamin billAh
(He who trusts La God). HAriln further stipulated that
Ma'mdn should have as his share, during the lifetime of
his brother, the government of the eastern part of the
empire. Each of the parties concerned swore to observo
faithfijiUy every part of this deed, which the Caliph caused
to be hung up in the Ka'ba, imagining that it would bo
thus guaranteed against all violation on the part of men.
These precautious were to be rendered vain by the perfidy
of Amfn. We shall see hereafter how he kept his oath,
and how he expiated his treachery by death.
It was in the following year, at the very moment when
the Barmecides thought their position most secure, that
HArdn brought sudden ruin upon them. The causes of
their disgrace have been differently stated by the annaUsts.
Some relate that the Caliph, preferring to all other society
ti::t of his sister "AbbAsa and of Ja'far b. YahyA, resolved
to unite them in marriage, in order to be able to bring
ti.em together in his presence without a breach of etiquette.
Ilo' meant, however, that Ja'far should continue to bo
only the nominal husband of hia, sister. Ja'far acceptei
this condition, but it was not long before he forgot it,
and the Caliph learned that his sister had given birth to a
son. This, it is said, was the cause of Ja'far's disgrace,
which involved his father !!.nd his brother. This story
may bo trae ; but the principal cause of , the fall of the
Barmecides appears to ■ have consisted in the abuses of
power of which they had been guilty, and- in the sovereign
influence which they exercised on those around them.
The Barmecides lived in a magnificent palace opposite to
that of the Caliph. Seeing one day an extraordinary crow d
around tho dwelling of liis first minister, HArun was movw'd
to say : " Verily YahyA has taken all business into his
own hands ; he it is who really exercises supreme power ;
as for me, I am Caliph only in name." This secret dis-
satisfaction was increased by a new act of disobedience
on the part of Ja'far. HAriin had ordered him to put to
death secretly a member of the house of 'All, whose
intrigijes he dreaded. Ja'far allowed the victim to escape,
and afterwards swore to the Caliph that his orders had
been executed. Soon after, however, information against
him was given to HArun, who, after compelling Ja'far to
acknov/ledge the truth, had his head struck off and brought
to him by Masrur, the chief of his eunuchs. On the very
next day \'ahyA, his son Fadl, and all the other Barme-
cides, were arrested and imprisoned ; all their property
was confiscated ; and HAriin chose as his prime minister
Fadl b. Eabi", who had been his chamberlain.
in the same year, a revolution broke out at Constan-
tinople, which overthrew the Empress Irene, and raised
Nicophonis to power. Tlie new emperor had scarcely
ascended tho throne, when he thought himself strong
euouqh to refuse the payment of tribute, and wrote an
insulting letter to HArun, who contented himself with
replying: "Thou shalt not hear, but see, my answer."
He then assembled an army, entered Asia Minor, and
took Heraclea, phmdering and burning along his whole
line of march, till Nicephorus, in his alarm, sued for
peace. Scarcely had the Caliph returned into winter
quartei-s, when Nicephorus broke the treaty. Notwith-
standing tho rigour of the season, HArun retraced hia
steps, and this time Nicephorus was compelled to observe
his engagements. The year after, A.n. 189 (a.d. 804-
805), disturbances arose in KhorAsAn. They were caused
by the malversations of tho governor of that province,
'AH b. 'IsA, and tho. Caliph went in person to Mcrv to
judgo of tho reality of the complaints which had reached
him. 'All b. 'IsA hastened to meet the Caliph on his
arrival at Ray. He brought with him a great quantity
of presents, which he distributed with such profusioo
ABaitWO.]
MOHAMMEDANISM
583
among the courtien that every one found a thoxisand
reasons for excusing hia conduct, llinin confirmed him
in hia p<3at and returned to Baghd&d, through which, how-
ever, he only passed, and went on to Ra^^ on the
Euphrates, a city which became his habitual residence.
He did not long enjoy the repose which he went there to
seek, for Nicephorus again broke the treaty of peace, and
the CaGph was obliged to take the field anew. Once
more Nicephorus was beaten, and so completely that he
was obliged to submit to the very harsh conditions which
th^ victor imposed on him.
Two years later, new disturbances broke out in Khori-
sin, where a certain Eifi' b. Laith had revolted. Hiriln
set out again for that province, accompanied by bis son
Ma'miin. It was to be his last journey. He was attacked
by a tumour in the abdomen, and struggled in vain against
this malady, which carried him off a year after his depart-
ure, A.H. 193 (a.d. 808-809), just on his arrival at the city
of Tus, the birthplace of the great epic poet of Persia,
Firdaust Hinin was only forty-seven years of age.
6. On the death of HAnin, his minister Fadl b. Rabf
.hastened to call together all the troops of the late Caliph,
and to lead them back to Baghddd, in order to place them
in the hands of the new sovereign, Amln. He even led
back the corps which V7as intended to occupy KhorisAn,
and which ought to have fallen to the share of Ma'miin,
according to the testament of Hinln. Fadl b. Eabf thus
committed a serious violation of the rights of Ma'miin ; but
be cared little for this, being chiefly desirous of vrinning
the confidence of the new Caliph. He was quite aware,
however, that in thus acting he was making Ma'miin his
irreconcilable enemy ; and he therefore purposed to use
every endeavour to arouse against biTn the enmity of his
brother Amin. He advised him to exclude Ma'miin from
the succession, and the Caliph was weak enough to listen
to him. Receiving the order to resign his government of
Khoris.ir. and to repair to Baghdid, Ma'miin was greatly
perplexed ; but his tutor and vizier, Fadl b. Sahl, reani-
mated his courage, and pointed out to him that, if he
obeyed the orders of the Caliph, certain death awaited him
at BaghdAd. Ma'miin resolved to hold out against Amln,
and found pretexts for eluding the orders of his brother
and remaining in Khorisdn. Amln, ih his anger, caused
the testament of his father, which, as we have seen, was
preserved in the Ka'ba, to be destroyed, declared, on his
own authority, the rights of Ma'miin to the Caliphate to
be forfeited, and caused the army to swear allegiance to
Ms own son MiisA, a child five years of age, on whom he
bestowed the title of Nitik bil-Hakk, "He who speaks
according to truth " (a.h. 194, a.d. 809-810). On hearing
the news, Ma'miin, strong in the rightfulness of his claim,
retaliated by suppressing the Caliph's name in all public
acts. Amln immediately despatched to Khorisin an army
of fifty thousand men, under the command of 'All b. 'tsi.
Ma'miin, on hia side, raised troops among his faithful
people of KhorisAn, and entrusted their command to TAhir
b. Hosain, who displayed remarkable abilities in the war
that ensued. In the following year, the two armies met
under the walls of Ray, and victory declared for TAhir.
Ma'miin now no longer hesitated to take the title of Caliph.
The year after, Amln placed in the field two new armies,
commanded respectively by Ahmed b. Mazyad and "Abd-
allAh b. Homaid b. Kahtaba. The skilful TAhir b. Hosain
succeeded in creating divisions among the troops of his
adversaries, and obtained possession, without striking a
blow, of the city of HolwAn, an advantage wbich placed
him at the very gates of BaghdAd. Ma'miin immediately
sent Tahir reinforcements under the orders of Harthama
b. AVan, which enabled him to maintain a firm hold on
All the conquered territory, and to continue his victorious
march to the capit&L Reverses naturally lead to fresh
reverses. One aJEter the other the provinces fell away
from Amln, and he soon found himself in possession of
BaghdAd alone, which was speedily invested by the troops
of TAhir and Harthama. That unfortunate capital, though'
blockaded on every side, made a desperate defence for two
years. Ultimately the eastern part of the city fell into
the hands of tiiiii, and Amln, deserted by his followers,
was compelled to surrender. He resolved to treat with
Harthama, as he hated TAhir; but this step caused his
ruin. TAhir learned by his spies that Harthama was to
receive the Caliph in person, and gave orders to a body of
horsemen to arrest Amtn as he issued from BaghdAd under
cover of the night. On the banks of the Tigris, Harthama
awaited Amln with a boat, but scarcely had the Caliph set
foot in it, when the agetits of TAliir poured on it a storm
of arrows and stones. The boat sank, and the Caliph had
to make his escape by swimming. But he was clocely
followed up, and had scarcely left the river when he fell
into the hands of his enemies, who shut him up in a hut
and went to inform TAhir of the capture. The victorious
general immediately ordered him to be put to death, and
the order was carried out. The head of the unfortunate
Amln was cut off and sent to Ma'miin, a.h. 1 98. It was
presented to him by his vizier, Fadl b. Sahl, surnamed
Dhii '1-RiyAsatain, or "the man with two governments,"
because Jus master had committed to him both the ministry
of war and the general administration. Ma'miin, on see-
ing the head, hid his joy beneath a feigned display of
sorrow.
7. On tne day following that on which Amln had JU'mun,
perished so miserably, TAhir caused Ma'miin to be pro-
claimed at BaghdAd. The accession of this prince appeared
likely to put an end to the evils of civil war, and to
restore to the empire the order necessary for its prosperity.
It was not so, however. The reign of Ma'miin — that
reign on which art, science, and letters, under the patron-
age of the Caliph, threw so brilliant a lustre — had a verj-
stormy beginning. Ma'miin was in no haste to remove
to BaghdAd, but continued to make Jlerv his temporarj'
residence. In his gratitude to the two men to whom he
owed his throne, he conferred on TAhir the government
of Mesopotamia and Syria, and chose as prime minister of
the empire Fadl b. Sahl, who had been already his vizier
in the government of KhorAsAn. The adherents of "AH
seized on the elevation of Ma'miin to power as a pretext
for fresh revolts at Mecca, at Medina, and in 'IrAk. At
Cufa a certain Ibn TabAtabA also broke out into open
rebellion, and placed an army in the field under one of
his .partisans, Abii '1-SarAyA. Hasan b. Sahl, brother of
Ma'miin's prime minister, who had been made governor
of all the provinces conquered by TAhir, immediately sent
troops against Cufa. "They were defeated, and Abii 'I-
SarAyA, encouraged by this first success, and no longer
finding a secondary part sufficient for his ambition,
poisoned his chief Ibn TabAtabA, and put in his place
another of the family of 'All, Mohammed b. Mohammed,
whom, on account of his extreme youth, he hoped to
govern at his will. Fresh troops sent against Abii '1-
SarAyA fared no better than the first, and several cities of
'IrAk, as Basra, WAsit, and MadAin, fell into the hands of
the rebels. Abii '1-SarAyA was already marching 'against
BaghdAd, when Hasan b. Sahl, in great alarm, hastily
recalled Harthama b. A'yan, one of the heroes of the civil
war, who was already on his way back to Merv. As soon
as this general had returned from KhorAsAn, the face of
affairs changed. The adherents of 'All were everywhere
driven back, and the whole of 'IrAk fell again into the
hands of the "AbbAsid?. Cufa was taken by assault, and
both Abii 'l-SarAyA and Mohammed b. Mohammed were
584
M O H A M M E D A N 1 S M
[ ABBA2IDS.
made prisoners. Thu loimer had his head struck off; the
latter was sent to Khorisin. The revolt in Arabia was
also quickly stifled, and it might have been supposed that
peace was about to be re-established. This, however, was
by no means the case. The civil war had caused a swarjn
of vagabonds to spring, Ps -it were, from underground at
Baghdad. They proceedtii to treat the capital as a con-
quered city ; and such was their audacity that they
plundered houses and cairied off women and children at
mid-day. It became necessary for all good citizens to
organize themselves into a regwlar nulitia, in order to
master these luffians. Meanwhile, at Merv, Ma'miin was
adopting a decision which fell Uke a thunderbolt on the
'Abbisids. In A.H. 201 (a.d. 816-817), under pretence of
jiutting an end to the continual revolts of the partisans of
'AH, and acting on the advice of his prime minister, Fadl,
bo publicly designated as his successor in the Caliphate
"All b. Milsi, a direct descendant of Hosain the son of
'AH, and proscribed black, the colour of the 'Abbisids, in
favour of that of the house of 'AH, green. This step was
well calculated to delight the followers of 'AH, but it
natmally could not fail to exasperate the "Abbisida and
their partisans. The people of Baghdid refused to take
the oath to 'All b. Miisi as heir-presumptive, declared
Ibrdhiui Ma'miin deposed, and elected his uncle Ibrihlm, son of
'i hi( ^^''■'"i'l to the Caliphate.'- The news reached the Caliph
iiecteJiit°"'y iudii-ectly, for his minister Fadl, desiring to leave
IlcighiUA Ma'mi'in only the shadow of power, kept all important
events carefully from his knowledge. The eyes of the
Caliph were opened, and he now perceived that Fadl had
been treating him as a puppet. His anger knew no
bounds. Fadl was one day found murdered, and 'All b.
Mi^si died suddenly. The historians bring no open accu-
sation against ila'miin of having got rid of these two
personages ; but it seems clear that it was not chance that
did him such a seasonable service. . Ma'miln of course
affected the profoundest grief, and, in order to disarm
susjncion, appointed as his prime minister the brother of
Fadl, Hasan b. Sahl, whose daughter BirAn he also after-
wards married. But on the other hand, in order to quiet
the people of Baghdad, he wrote to them : "The cause of
V'Ur dis.'atisfaction in the business of 'AU b. MiisA no
longer exists ; since ho who was the fibject of your resent-
ment li.is just died." From that moment the pseudo-
calipli Ilir.Ahlm found himself deserted, and was obliged
to seek safety in concealment. His precaiious reign had,
however, lasted nearly two years. Ma'mi\n now decided
on tiiaking a iniblic entry into Baghdad, but to show that
lie came as a master, he still displayed for several days
the green flag of the house of 'AH, though at last, at the
rntrcaty of his coiuticrs, he consented to resume the black.
From this time the real reign of Ma'nnin began, freed as
lie now was from the guardianship of Fadl. His general
TAliir alone ro\itiiuuHl to excite his su.'picions. Under
the pretence that he could no longer endure the sight of
the murderer of liis brother, he removed T.ihir to a dis-
tance by apiKiinting him governor of Khor.'lfAn. Like most
of the grcit Moslem generals, T'^hir, it is said, conceived
the project of creating an independent kingdom for himself.
His death, A.n. 207, prevented its realization ; but as his
descendants succrcdeil liim one after the other in the post
of governor, ho may be said to have really founded a
dynasty in Khor;W;in. When, two years later, the imiiostor
B.-ibak set up a communi.stic sect in Armenia and Azcr-
baijAn, it was a son of X'lhir, 'Abdalhlh, who was commis-
nioneil by Jla'muM to put him down. Notwithstanding his
ibility, 'AlxlalhUi could not accomplish the task, and it
'« (I TcnKirVal'le cssnv by Bnitncr Uo Aleyuarvl, iu
. for March Ai.lil. IMS).
was only under Ma'mun's successor that B.'ibak vfas taken
and put to death.
Ever since Ma'miin's entry into Baghdid, the pseudo-
caliph Ibrihlm had led a wandering life. He wn»
arrested one night in Baghdid, under the disguise of a
woman, and brought before Ma'miin. The latter gener-
ously pardoned him, and also granted an amnesty to the
former minister of Amfn, Fadl b. Rabf, although he had
been the chief promoter of the terrible civil war which had
so lately shaken the empire. After that time, Ibrihlm
the son of Mahdi lived peacefully at the court, cultivating
the arts of singing and music, in which he excelled.
Tranquillity being now everywhere re-established, ila'-
miin gave himself up, without hindrance, to his scientific
and literary tastes. He caused worka on mathematics,
astronomy, medicine, and philosophy, to be translated
from tie Greek. It was also by his orders that two
learned mathematicians undiertook the measurement of a
degree of the earth's circumference. Ma'miin interested
himself, too, in questions of religious dogma. Shocked
at the opinion which had spread among the Moslem
doctors, that the Koran was the uncreated word of God,
he published au edict' commanding them to renounce this
error. Several distinguished doctors, and, among others,
the celebrated Ibn Hanbal, founder of one of the four
orthodox Moslem sects, were obliged to appear before an
inquisitorial tribunal ; and as they persisted in their
belief respecting the Koran, they were thrown into prison.
Meanwhile, war having broken out between the Greeks
and the Moslems, Ma'miin set out for Asia Minor, to put
himself at the head of his army. On his arrival at Tarsus,
he received from the governor of Baghdid the lepoit of
the tribunal of inquisition, and ordered that the culprits
should be sent off to him. Happily for these unfortunate
doctors, they had scarcely started on the road to the
frontiers, when news of the Caliph's death reached
Baghdid. Ma'miin having bathed in the Podendon, a
burning fever was the result, which brought him to tha
grave in A.H. 218 (a.d. 833). Before his death, ho
designated as his successor his brother Mo'tasim bilhUi,
(He who seeks defence in God), whom he had for a long
time preferred to Mo'tamin.
8. The accession of the new Caliph Motasim met at Motatia
first with active opix)sition in the army, .where a powerful biUii.
party had been formed in favour of "Abbds, the son of
Ma'miin. Thanks, however, to the disinterested conduct
of that prince, civil war was averted. 'Abb:i3 publicly
renounced all pretension to the Caliphate, and took the
oath of allegiance to his uncle. Mo'tamin, the son of
H.'lriin, imitated the conduct of 'Abbis, and the whole
army accepted Jlo'tasim, who made his public euti7 into
Baghdid in the month of Ramadan 218.
The new Caliph, far from putting a stop to the persecu-
tion which had been directed against the orthodox doctors,
took up and carried out the views of Jila'mun. The
doctor Ibn Hanbal was beaten with roils and tlnon-n into
jirison, together with several of his companions, and waa
not restored to liberty till the Calijihato of Motawakkil.
This persecution h.id already prejudiced the jieople against
Mo'tasim, and their discontent became more marked wlicii
the Caliph created a new body of troops, specially intended
to watch over his jiei-son. This new guard was composed
of Turks, an unbridled and undisciplined liody of soUliciy,
who, moreover, held in open contempt the religious pre-
cepts of Islam. Tired of the excesses of every kind com-
mitted by the Turk.i, the people of BaglnhUl rose in
insurrection, and Mo't.iKi?n, net daring to act with severity
cither against his guard or the citizen.-^ took the rourso cM
quitting tlio city. I.eavini; tlie governiiieiit of the rnpitol
in the hands of his son AV.'ithil; billih (He who trusts iu
y.i»«fRma J
MOHAMMEDANISM
585
God), he cslaUisiicd hisrself n-ith lu3 guard at S¯a, a
small placo situated a few leagues above Baglid&d, and
changed its name to Sona-man-ra'a (He rejoices who
sees it). This resolution of Mo'taaim was destined to
prove fatal to his dynasty ; for it placed the Caliphs at the
mercy of their 'Praetorians. In fact, from the time of
Mo'tasim, the Caliphate became the plaything of the
Turkish guard, and its decline was continuous. Some
glorious feats of arms, however, were still performed
under MoHasim. The sectary Bdbak was at last taken by
Afshin, a Turkish general of the Caliph, in the year 223
(a.d. 837-838). B4bak was carried to Baghdid, led
through the city on the back of an elephant, and then
delivered to the executioners, who cut off his arms and
his legs. Afshin, however, was -very ill revrarded for hie
aervices, for shortly afterwards the Caliph had him put to
death on a charge of heresy.
The death of Ma'miin had lor the moment suspended'
hostilities with Constantinople ; under Mo'tasim the war
was rekindled. A "valiant Greek general, Manuel, who
had incurred the displeasure of the Emperor Theophilus,
took refuge with the CaUph, who eagerly welcomed him
and gave him a command. Manuel began by reducing
Khor&sin, which had risen in revolt, and Mo'tasim was so
well satisfied with him that he thought of employing him
against his own countrymen. This was precisely what
Theophilus dreaded, and he took measures accordingly to
bring back the banished general to his side. He sent an
ambassador to Motasim, under pretence of ransoming
some Greek prisoners ; but the real object of his mission,
which he contrived to communicate to Manuel, was the
recall of that general. Manuel, feigning great animosity
against his country, himself asked to be allowed to lead a
Moslem army into Cappadocia. The Caliph granted his
request, and sent with him his own son Withi^ biUih.
But, as soon as they reached the frontiers of Cappadocia,
Manuel confessed to the young prince that his intention
was to return to Constantinople, and quitted the army.
Theophilus, taking advantage of the confusion into which
the departure of Manuel had thrown the Moslems, made
an incursion into Syria, laid waste that province as far as
Zabatra, and returned loaded, with booty. At the news of
this disaster, MoHasim assembled a formidable army,
estimated at more than two hundred thousand men,
penetrated into Asia Minor, beat the Greeks, and took
the city of Amorium, which, he ordered to be razed to the
ground. A revolt which broke out at Baghd&d in favour
of his nephew 'Abbis, "the son of Ma'miin, compelled the
Caliph to turn bact Mo'tasim had the unfortunate
'Abbis arrested, and he was soon after found dead in his
prison. Af o'tasim survived him oiJy four years. He died
at Sgrra-man-ra'a, in A.H. 227 (a.d. 841-842).
9. His'son Withi]^ who succeeded him, showed himself
no less intolerant on the doctrinal question of the un-
created Koran. He carried his zeal to such a point that,
on the occasion of an exchange of Greek against Moslem
prisoners, in the year 231 (a.d. 845-846), he ordered, that
all the Moslem captives who would not declare their
belief that the Koran was a human work, should be left
in the hands of the enemy. The reign of Withi^ bill4h
was not otherwi-w marked by any very striking events.
He died in 232 (a.d. 84G-847), after a reign of five years.
Ab he had appointed no successor before his death, the
principal personages of the state at first cast their eyes on
his son Slohammed ; but they had scarcely saluted him
with the title of Caliph, when they changed their purpose,
and offered the supreme power to Motawakkil 'ala '114h
(He who trusts to God), brother of Wdthilf. This prince
wa.<> therefore elected in the some year in which Withi^
died.
10. The first act of Motawakkil waa an atrocious Uot«-
cruelty. He seized Mohammed b. *Abd al-Melik, his*'':*^
brother's vizier, who .had always been his enemy, and
ordered him to be placed in a furnace bristling within
with iron points, which was then raised to a red heat.
The Caliph looked on at the agonies of his victim,
incessantly repeating : " Pity is a weakness." This had
been the favourite maxim of the unfortunate vizier. An
impostor named Mohammed b. Faraj had set himself, up
as a prophet, giring out that he was Moses risen from the
dead. By means of this gross fabrication, he had con-
trived to attract twenty-seven followers: The Caliph had
him seized, and condemned him to perpetual imprison-
ment ; but first he compelled each of the followers of
Mohammed to give the pretended prophet ten blows on
the head with his fist ; and the poor wretch expired under
the hands of his own disciples, (a.b. 235, A.D. 849-850.)
In the year of hia elevation to the Odiphate, Mota-
wakkil had regtilated the succession to the empire' in his
own family, by designating as future Caliphs his three
sons, Montasir billAh (He who seeks help in God), Mo'tazi
billih (Strong through God), and Mowayyad bilUh
(Assisted by God). In acting thns, his object was to
protest against the tendency of his predecessors to favour
the house of 'All, and to guard against the attainment of
the Caliphate by any member of that house. Motawakkil
displayed the most extreme hatred for the descendants of
the prophet. He even went so far as to destroy the
chapeT erected over the tomb of Hosain at Kerbelij and
forbade the ShTites to visit the spot. Not content with
attacking the liberty and the property of the descendants of
'All, he insulted their belief, by taking huffoons into his
pay, whose bvisiness it was to turn the person of 'All into
mockery. He also persecuted the Oiristians and the
Jews ; excluding them from all public employments, and
obliging them to send their children to Moslem schools.
In the year 237, a revolt brolce out in Armenia. The
Caliph sent the Turk Bugha against the rebels ; but they
met him with a vigorous resistance, and it was four years
befora peace was restored to the province. During that
time the Greeks effected a descent on Egypt, and Damietta
was taken and burned. Motawakkil caused Damietta to
be fortified, and transferred liis own residence to Damascus,
doubtless that he might be able to keep a clo-ser watch on
the proceedings of the Byzantines. He soon thought
himself strong enough to take the offensive, and poured
his Turkish soldiery into Asia Minor, where they
encountered the i>ame Manuel who had been formerly
received at the court of Mo'tasim. After an alternation
of sluccessea and reverses, both Moslems and Greeks
retired from the conflict. Motawakkil then returned to
his residence at Sorra-man-ra'a, and there caused a magni-
ficent quarter to be built, which he called Ja'fariyya,*
There he gave himself up to debaucheries ; till at last,
during one of his orgies, he was murdered by a Turkish
soldier named Wasif, who had been bribed to the deed
by his own son Montasir billih (a.h. 247,' a.d. 861-8G2).
11. On the very night of his father's assassination Itorv
Montasir had himself proclaimed CaUph. The conspirators *"■'"•
among the Turkish soldiery compelled him to deprive his
two brothers, Motazz and Mowayyad, who ■srere not agree-
able to thsm, of their rights of succession. Montasir did
not long enjoy the fruits of his crime. He died five
months after, by poison, it is said.
12. The 'Turki^ soldiery, which now arrogated to itself Kotti'itv
the mastery over the CaUphate, chose in suqpession to
Montasir his cousin Ahmed, who took the iitle of Mostafn
' That i\ " City of Ja'fkr." Ja'far was Motavakka'a own proper
taa.
XVL — 74
686
MOHAMMEDANISM
['abbasids.
•oillih (He who looks for help to God). Under the reign
of this feeble prince, the Greeks inflicted Berioua losses on
the Moslems in Asia Minor. The Turkish soldiery, instead
of attempting to repair these losses, revolted against the
Caliph whom they had themselves chosen, and plundered
the city of Sorra-man-ra'a. Taldng advantage of these
disorders, a descendant of 'AK, named Hasan, gained pos-
session of Tabaristin and JorjAn, and permanently deprived
the Eastern Caliphate of those provinces. At the same
time, insurrections sprang up in every part of tlie empire.
Next, the chiefs of the Turkish soldiery, in their mutual
jealousies, began to tear each other to pieces. The infatu-
ated Caliph fled from Sorra-man-ra'a, and took refuge at
Baghdad. The Turks now resolved on his destruction,
and forgetting that they themselves had deprived Mo'tazz
bilUh, brother of Montasir, of his legitimate rights, chose
him as their Caliph. They next placed at their head a
brother of Mo'tazz, named Mowaffalf billAh, and besieged
Mosta'in at Baghdid. At the end of one month (a.h.
252, A.D. 866), Mosta'in surrendered, and was put to
death.-
Mo'tazz. 13. Mo'tazz billAh, thus called to the throne by the very
men who had previously sought to exclude him from it,
resolved to free himself from the yoke of the formidable
Turkish soldiery which thus made and unmade Caliphs.
But to maintain a struggle against such terrible adversaries,
the new sovereign would have needed an ability and energy
which he did not possess. He made, indeed, a very
impolitic beginning in getting rid of his brothers Moway-
yad ^nd Mowaffalf, of whom he put the former to death,
and drove the latter into exile. Some time after, it is
true, he had the satisfaction of seeing Wasif, one of the
chiefs of the Turkish soldiery, lose his life in a mutiny of
■his own troops ; and, that of defeating in person another
chief, Bugha, whom he afterwards caused to be beheaded.
But in the following year (a.h. 254), the Turks chose as
Itheir leaders the sons of Waslf and Bugha, Silih and
Mohammed, who avenged their fathers by plundering the
palace of the prime minister and besieging that of the
Caliph, whom they seized and threw into close confine-
ment, where he died of hunger and thirst, A.H. 205.
Moht.i.'.i. 14. Immediately after the fall of Mo'tazz, the Turks
bi'ought from Baghdild one of the sons of Withik billAh,
and proclaimed him Caliph, with the title of Mohtadi billAh
(Guided by God). Mohtadi, a man of noble and generous
spirit, exerted himself, but in vain, to release his prede-
;essor from prison. Having failed in this, he kept the
precarious measure of power which his masters left
him, and applied it to the regeneration of Moslem
society, the decay of wliich appeared to him imminent.
He forbade wine and games of chance ; he devoted
himself to the administration of justice ; he examined in
person every sentenco passed by the judges, and gave
public audience to the people twice a, week for the redress
jOf their grievances. The farmers of the revenue were
isubjected to strict control, and the taxes were considerably
lighterjcd. It seeuicd as if these reforms were likely to
rc-eslablish order and prosperity in the empire. But
Mohtadi came too .ate, and the Turks did not leavp him
time to finish his work. ?i!ih, one of the chiefs of the
Turlcish soldiery, having been assassinated by a rival,
!Mohtadi punished the guilty person 'with rigour. Tho
Turks, in their rage, beset tho palsce and slaughtered the
unfortunate Caliph (a.ii. 256, a.d. 870).
Ht-\^- 15. Whether from weariness, or from repentance, the
"''''• Turkish soldiery discontinued for a time their hatefiJ
excesses. A son of Motawakki! \vo,ii brought out of prison
to succeed his cousin, and reigned 'or twenty-two years
under the name of Mo'lamid 'ala 'llMi (He whose support
is God). During hi? reij-n two great events took place,
tokens ana precursors of the dissolution of the Caliphatej
Eastern Persia and Egypt separated themselves by force
from the empire, and two uew dynasties established
themselves in these countries, those respectively of the
Safl'irids and the Tuliinids. The founder of the former,'
Ya'lfiib b. Laith, was the son of a coppersmith (§a!i;Vr).
At the head of a band of resolutem'en, he invaded succes.s-
ively Khorisin, Kirmdn, and Sijistin, and at last the Caliph
Mo'tamid, powerless to arrest his progress, was obliged to
give an official recognition to accomplished facts. But
Ya'kiib was not satisfied vrith this ; he soon possessed
himself of Tabaristin, FdrsistAn, and Ahwiz, and thence
marched against BaghdAd. Fortiine, however, deserted
him ; he was beaten in the neighbourhood of Wisit (a.h.
262), and compelled to return to Persia in order to levi- a
new army there. In 2G5 he resumed his march against
Baghdid, but was obliged by sickness to halt at Jondis-
dbiir, where he died ; not, however, till he had obtaij^ed
from the Caliph a formal investiture of all the provinces
he had conquered. He was succeeded by his brother
"Amr. On the other side, a certain Ahmed b. Tnliin, the
son of a freedraan, who had obtained from the Caliph the
post of governor of Egypt, planned the creation for himself
of an independent kingdom. Under Mo'tamid he even
invaded SjTia, and perhaps would have pushed his con-
quests still farther, had not death overtaken him in A.H.
270 (a.d. 883-884). His son Khomarilya succeeded him
in Egypt, and though, at a later period, he submitted to
pay tribute to Mo'tadid, nevertheless a dynasty had been
founded in that country which lasted for twenty-one years
longer. Mo'tamid died eight years after Ahmed b. Tiiluu.
16. The reign of Mo'tadid bilUh (He who seeks his Mots-
support in God), who succeeded his uncle Mo'tamid. is'?i^
principally remarkable for the rise of the celebrated feet
of the Carmathians (KarAmita), who for two centuries kid
waste the Moslem empire, and for the extinction of the
SafTArid dynasty in Persia, where it was replaced by that
of the SAmAnids. Some details respecting the origin and
the creed of tho Carmathians will be found in the third
section of this article. We shall content ourselves here with
stating the fact that these sectaries, who were numerous
in 'IrAk, Syria, and Eastern Arabia, kept in check all the
annies which were sent against them. Under the reign of
Jlo'tadid they invaded Mecca and committed great ravages
there. In A.n. 281, Mo'tadid repaired the disasters which
they had caused there, and raised important works about
tho Ka'ha. Mo'tadid died in 289 (a.d. 902), leaving
the throne to his son Moktafi billAh.
17. Moktafi billAh (He who sufficeth himself in God) Kcltifi
reigned for six years, during which he had constantly to
struggle against the Carmathians. One of his generals,
indeed, gained a signal victory over these sectaries ; but, to
avenge their defeat, they lay in wait for a caravan which
was on its return from Jlecca, and massacred, twenty
thousand pilgrims. This horrible crime raised the whole
of Arabia against them. The Carmathians were beaten
again, and Dhikri'iya, one of their ablest generals, was
tal. -n and put to death. The sectaries remained quiet for
sc .le time, and tho Caliph took advantage of this respite
to take Egj'pt from tho house of "TMliin, and to confer its
government on tho Ikhshldites. Moktafi died A,a. 295
(a.d. 907-908). His activity and energy revived for a
moment the prestige of the Caliphate; but this fleeting
renev/al of its greatness was soon to disappear, and decay
resumed its course.
18. The new Caliph, Moktadir billAh (Powerful through Holtt»-
God), was only thirleen years of ago when he ascended ^■^^
the throne. His extreme youth prejudiced tho people of
BaghdAd against him : they rebelled, r.nd r.v;ore ailcgiance
to 'AbdallAh, son of the forme;' Colinh Uo'iaiz ; but the
"ABBA'SICS.J
MOHAMMEDANISM
587
"ITie 7k
Toe hs
Bids.
Efflrr,
party of Molftadir prevailed, and bia rival was put to
death. Molftadir, however, was too young to exercise
any real power ; he was governed by his eunuchs. He was,
besides, a man of feeble character, and looked on help-
lessly at the death-struggle of the empire, upon which
calamities of every kind now poured in. The Greeks
invaded Mesopotamia. A truce was concluded with them;
but the Carmathians then recommenced their disorders in
Syria. The indolence of the Caliph, and lus inaction in
the face of this danger, alienated all hearts from him ; and
the eunuch Miinis, the principal chief of his party, took
the lead in deposing him and proclaiming in his stead his
brother KAhir biMh (Victorious through God), in the
year 317 (a.d. 929-930). ?ihir, however, having refused
to distribute a donative to the army on the occasion of his
accession, a counter-revolution took place, and Moktadir,
who had been imprisoned, was taken from his dungeon
and replaced on the throne, only three days after his de-
position. Favoured by these distvu-bances, the governor of
Mosul, Nisir al-DaulS, declared himself independent, and
founded definitively the djmasty of the Hamdinites ; thus
causing an additional dismemberment of the empire. The
Carmathians,in their turn, under the guidance of a new chief,
Abii T^hir, obtained possession of Mecca, and carried off
the celebrated black stone of the Ka'ba, which they did not
restore till very long afterwards. Meanwhile the eunuch
Miinis had been disgraced. He withdrew at first to Mosul,
to the court of Niisir al-Daula ; but it was to raise an
army and march upon Baghdid, where the Caliph had
again fixed his abode. The object of Miiuis was not to
attack the Caliph, but only to take vengeance on his
personal enemies. Molftadir was induced by evil coun-
sellors to make a sally against Mi5.ms. His troops were
put to the rout, and he himself fell on the field of battle,
'n the year 320 (a.d. 932).
With the reign of Molftadir is connected one of the
greatest events in the history of the Caliphate, the founda-
tion of the F4timite dynasty, which reigned, first in the
Maghrib and then in Egypt, for nearly three centuries.
The first of this family who put forward any pretensions
to the Caliphate was 'Obaid Allih, aumamed the Mahdl, or
Messiah of the followers of 'AU, who gave himself Out as
a direct descendant of 'All, through his wife Fitima, the
daughter of Mohammed, vfhence the name of Fitinfdte. It
seems to be proved that 'Obaid AHAh was really descended
from a certain 'Abdallih b. Maimun el-Kaddih, the
founder of the Ismailiar. sect, of which the Carmathians
were only a branch. This "Obaid AllAh had himself
become pontiff of the Ismailians. As early as the Caliphate
of Moktaff, one of 'Obaid Allih's missionaries, named
Ab\i 'Abdallih, had succeeded in gaining numerous parti-
sans in the province of Africa, then subject to the
Aghlabites, and the victories of this missionary had
wrested Eastern Africa from the family of AgUab when
Moktadir ascended the throne. 'Obaid AllAh then
repaired to his new realm (a.H. 303), and founded the
city of Mahdfya, which he made his capital. He tried
also, but without success, to seize Egypt ; the conquest of
that country was reserved for one of his successors, Mo'izz
U-dinillih. "Obaid All&h died two years after Moktadir,
leaving to his son K&im an empire already sufficiently
powerful to cause uneasiness to the "Abbisids, to the
Omayyads of Spain, and to all the Christian princes
whose states bordered on the Mediten-anean.
19. KAhir bUlih, on being raised anew to the throne
after the death of his brother Molftadir, still bore ill-wiU
to his patrons, and tried to free himself from their
guardianship. The emirs of his court dethroned him a
second time and put out his eyes. One of hie nephews
was then proclaimed Caliph \inder the name of RAdJ
bill4h (Content through God). This prince, who was
entirely governed by those about his person, created,
in favour of a certain Abiibekr Mohammed b. RAik, the
office of Amir al-0mar4, or F.mir of the Emirs, which
nearly corresponds to that of Mayor of the Palace among
the Franks.! fhe Amir al-Omard was charged with the
administration of civil and military affairs. He also acted
as the Caliph's deputy in sacerdotal functions, and was
named next after him in the public prayers. Thenceforth
the Caliphate was no longer at.ything but an empty
shadow. During the reigns of KAhir and-EAdI, the Car-
mathians became more audacious than ever. The Am(r
al-0mar4 was obliged to purchase from them the freedom of
pilgrimage to Mecca at the price of a disgraceful treaty.
Thus the Caliphate found itself almost reduced to the pro-
vince of BaghdAd. KhorisAn, Transoxiana, Kirmi^n, and
Persia were in the hands of independent sovereigns, the &i^
minids, the Biiyids, and a prince named Washimgir. The
Hamdinites possessed Mesopotamia; the SAjites, Armenia;
Egypt was under the rule of the Ikhshidites ; Arabia was
held by the Carmathians ; Africa, as we have seen, had
become the prey of the FAtimites. The single transient
success obtained by ^&di was the capture of Mosul in a.h.
328 (a.d. 939-40) ; and even this success he owed to the
Turk Bejkem, who had succeeded Mohammed b. B&ik as
Amir al-OmarA.
Ridl died in fte following year, and was succeeded by Mottakl
Motta^:! lillih (He who fears God). From his very
accession, this prince saw himself exposed to the attacks
of a certain Al-Baridl, who had carved out for himself a
principality in Chaldsea, and who now laid siege to Baghdid.
Nisir al-Daula, prince of Mosul, who had been reinstated in
his government, offered an asylimi to Mottakl; put his
troops at his disposal, and succeeded in repelling Al-
Baridl. In return he obtained the office of Amir al-OmarA.
But there were other competitors for that post. Tur;in,
a former lieutenant of Bejkem, protested sword in hand
against the choice of the Caliph, and threatened Bagh-
dAd. Ikhshid, sovereign of Egypt, offered Mottakl a
refuge in his states ; but Turun, fearing to see the Caliph
obtain such powerful support, found means to entice
him to his tent, and had his eyes put out, a.h. 333
(a.d. 944-945).
As successor to Mottakl, Turuij chose Mostakfl billih (He llotX'Mfi.
who places his whole trust in God). This prince, like his
predecessors, was a mere puppet in the hands of his min-
isters. A new Amir al-OmarA, Zlrak b. Shirzdd, made
himself so hateful to the people of Baghddd by his deeds
of violence and rapacity that they besought the help of
the Biiyids. Ahmed, the third prince of that dynasty,
entered BaghdAd, overthrew Zlrak, and took his place
under the title of Mo'izz al-Daula. Mostakfl soon had
enough of this new master, and ventured to conspire
against him. The plot was discovered, and Mo'izz al-Daula
had the eyes of the Caliph put out. There were now at
BaghdAd three Caliphs who had been dethroned and
blinded — KAhir, Mottalpt, and Mostakfl. Mo'izz al-Daula
thought for a moment of restoring the illusory title of
Caliph to the descendants of 'AU. He feared, however,
lest this should lead to the recovery by the Caliphs of
their former supremacy, and his choice feU on a son oi.
Moktadir under the name of Motl' UUAh (He who obeys Moti".
God). Reserving to himself all the powers and revenues
of the Caliph, he allowed Motl' merely a secretary and a
moderate pension. The prince of Mosul, wlio began to
think his possessions threatened by the neighbourhood of
Mo'izz, entered on a struggle with him and tried to wrest
BaghdAd from him; but he failed, and was obliged to
> See Defrdmery, Uimoire aur la Emirt al-Omlra Pari3.-«18^
588
MOHAMMEDAN. ISM
['abbIsiss.,
submit to tho payment of tribute. We have said above
that Mo'izz al-Daula professed a great veneration for the
house of 'All. His preference showed itself in public acts.
He caused tho most terrible imprecations against the
Omayyads to b'e posted up at the doors of tho mosques.
This step irritated men's minds ; and a general insurrec-
tion was imminent at Baghddd, when Mo'izz died (a.u.
3.')6), leaving his power to his son 'Izz al-Daula.
^Vhil6 the 'Abbdsid family was thus dying out in -shamo
and degradation, the FAtimites, in the person of Mo'izz
H-dfn-iU.lh, were reaching the highest degree of power
and glory (see Egypt, vol. viL p. 750 sqq.) Jauhar, a
general of Jlo'izz li-dln-Uliih, conquered Egypt for his
master, and Arabia acknowledged tho sovereignty of tho
Fdtimites.: The Cannathiaiis, who had so long contended
against t!;e 'Abbdsids, nov/ came to better terms with
Mote, and their general made tho Caliph the offer of
driving back the Fdtimites, on condition of his granting
him the government of' Egypt. Motf preferred to stand
neutral in tho struggle ; and tho Carmathian general, who
with the support of Motf might perhaps have triumphed
over Mo'izz, was beaten by his powerful rival Moti',
Laving ' been struck, by paralysis, was obliged to abdicate
in the year 363 (a.d. 973-974), and loft the empty title
Tii'. cf Caliph to his soa T^i' liramr-illih (Obedient to the
coiiunr.nd of God). Tho new Caliph lived at &-st in
peace, for It was now the office of Amfr al-Omard which
provoked 01-will. 'Under the reign of 'JCii' the Biiyid
princes contended furiously with one another for the office
of Emir, and one of them, 'Adod al-Dan!a, having con-
quered 'Izz al-Daula, took tho title, never before employed,
of Sh.^hinshAh, or king of Jdngs. ^On his death ho trans-
mitted his office to his threo sons, who held it successively,
under the names of Shams al-Daula, Sharaf al-Daula, and
Bahd al-Daula. The last, "who was as avaricious aa he
was ambitious, took oITence at tho Caliph T4i' for having
dispo.>;ed of certain sums of money, of which he wished
to reserve tho manaeement to himself, compelled him to-
abdicate in a.h. 381, ana replaced him by a grandson of
Molftadir, who took tho name of KAdir billdh (Powerful
through God), and reigned forty one years under the
tutelage of the Biiyids. ' Meanwhile events were pre-
paring the fall of the Biiyids. In Persia, Mahmiid of
iGhazni was founding the powerful empire of tho Ghaz-
'ncvidsj^ which extended to the Indus, and the Seljilk
Turks. were already invading Khorisdn. It was under
tho successor of KAdir billih that that sanguinary revolu-
tion took place, which was to give over the government
of Baghdad to tho SeljulfS.
Kiia. lyiuir billih died in jtli.-. 422 (a.d. 1030-31), and
■was succeeded by Kaim bi-amr-Lllih (He who is charged
with tho business of God). Tho new Caliph, groaning
under the iron hand of his' Amir al-Omard, called to
his aid the Seljiilj: Toghril Beg, who entered Baghddd
in the jnonth of Ramadan in the year 447 (a.d. 1055-
1056), overthrew tho Biiyids, and took their place. Some
years later, Toghril married the daughter of the Caliph.
At bis death, Toghril left to his nephew AJp ArslAa
tho .title of Sultan, a flourishing empire, and unco'
trolled pd'wer. As for Kiim, he enjoyed the Caliphato
in peace under the tutelage of Alp ArsUn and of Ids
succcisor Malifc SbAli, till his death in a.h. 467. His
•^■'iktucL'. grandson, Mpktadl bi-anir-illAh (He who obeys the orders
of God), who succeeded him, owed to the power of Llalik
Sh.'ih the honour of recovering his supremacy in Arabia.
At Medina and Mecca his name was substituted in the
public prayers for those of the Fdtiniito Caiiphs. This
was, after all, a mere gratification to his vanity, for Malilc
ShAh was the real sovereign, and the Caliph thought
himself highly honoured in marrying , the daughter of his
powerful patron. This union, however, far from drawing
claser the bonds of friendship between Malik Shih and
Molftadl, became on the contrary a cause of strife. The.
Caliph having put away his wife, who had wearied him
by her peevish humours, was compelled by Malik, Shih to
appoint the child whom he had had by her as his successor,
to tho prejudice of his eldest son. MaUk Shdh also exiled
his son-in-la,w. to Basra.' Just, however, as this order was
about to be carried out, Malik , ShAh died. MoUtadl
survived him only a few months. It was during tie
• reign of his successor Mostazhir billih' (a.h. 487-512) that Most'^
the first crusade took place. We need not here enter ^ '''•'*
into tho details of those wars. It is sufficient to say thatS"!'"'
from the date of the first crusade Baghdad ceases, so to
speak, to have any special hjstoiy. The successors of
Mostazhir billih (Ha who seeks to triumph througli God)
were — Mostarshid billih (He who asks guidance from God),
A.H. 512-529 ; KAshid billih (Just through God), a.h. 529-
530; Mo^tafl h-amr-illih (He who follows the. orders of
God), A.H. 530-555 ; Mostanjid billih (Ho who invokes
help from God), A.H. 555-566 ; and Mostadl' bi-amr-UlAh
(He who seeks enlightenment in the orders cf God), a-H.
566-575. . Under this last, the Fitimite dynasty v.-as at
length destroyed, and Egypt fell again under the spiritual
authority of the CaUpha of Baghdid. It was one of the
generals of the Emir Nilr al-din, the celebrated galdh al-
dln (Saladin), who made this important conquest in A.n.
567 (a-D. 1171-1172). Ho maintaip-ed himself in Egypt
as Sultan, founded a new dynasty, that of the AyyubiteSj'
and in some sort compelled Nisir li-dln-ilUh (Ho who
helps the religion of God), the successor of Mosl»ii' (a.h.
575-622),, to acknowledge his title and to ratify his
usurpation;
A still more formidable danper was now threatening T!i«
Baghdid. The tenible Jinghlz Khin was issuing from Mongols
the depths of Asia at the head of his Mongols, and was
beginning to invade I'ransoxiana. Under Ndsir li-dln-
illih's successors, Zdhir billdh (Victorious through God),
A.n. 622-623, and Mostansir billdh (He who asks help
from God), a.h. 623-640, tho Mongol invasion advanced
with immense strides ; and when, after them, Mosta'sim
billdh (Ho who seeks his defence in God) was named
Caliph in tho year 640 (a.d. 1242-1243), the last days of
tho Caliphato bad arrived. Huligu; Vv'ho was then sove-
reign of the Mongols, determined to make himself master
of the whole of Western Asia. . He placed himself at tha
head of his immense hordes, swept everything ucfore hira
on his march, and arrived under the walls of Baglid.dd.
In vain didi- Mo.sta'sim sue for peace. The siege was
actively piusued, and on the 29th of Moharram 6S(» (0th
February 1258), tho Mongols forced their way into
Baghd/id and planted the standard of HuIiVgu on tlio
highest of its towers. Tho city was given up to fire and
slaughter ; Mosla'.sim was thrown into prison, and died
there a few days after ; and with him expired the Eastern
Caliphate, wh;.ch had .lo-sted C26 years, from the deaUi of
Mohammed.
In vain, three years later, did a scion of the race of tha
Abbasids, who had taken refuge in Egj-jjt, make an effort
to V ■'■ore ti, dynasty which ■was now for ever extinct. At
the h'ead of a few followers, be marched against Baghdid,
but was repulsed by tho governor of that city, and died
fighting. At a later period, another descendant of the
'Abbdsids also sought an asylum in Egypt. Tho Sultan
Baibai's, after a judicial investigation of his origin, pro-
claimed him Caliph under the name of Hikim bi-amr-illihv
His sons inherited this empty title, but, like their father,
remained iu Egypt, ■without power or influence. This
shadow of sovereignty continued to exist till the conquest
of Jigypt by the Turka
ursnruTioKi!. ]
MOHAMMEDANISM
589
GiMZ&LooicxL Tabu of tbb 'AsbXsid Califbi vovm to tbb
Fau, or Baobsas.
'AbUU.
■AbdalUh.'
•Ak
Ibiiugi. L Abd 'l-'Abb^ 2. Uanair.
• 8. HthiU.
_J
4. H4di.
B. HanSn al-Rashid.
6. Amin. 7. Ua'miis. 8. Mo tasiin.
Mohammect 9. WatUk. 10. MotawakkiL
I I ° I
12. Mosta'in. U. Mohtadi.
UowafUc. 11. Montasir. 15. Mo'tamid. 13. Motazz.
6. M<
.o'tsdid.
18; Moktadir.
r
17. MoktaC
I
■22. Mostakfi.
Ishdk. 2S. Hotf. 21. MottaJd.
25. Kadir.
26. Kiim.
M. Tii'.
rw
Moluunxned Dhakliirat ol.Din* ^
27. MoktadL
r
28. Mostafhir.
«L Uoktafi. 2«. Mostanhid.!
ii. Moetasjid. 30. Ziahii.
33. Mostadi'.
31. IT&sir.
36. Z&hir.
I
36. Uoataiuir.
37. UoiU'nm.
SicT. TTT, — Sketch op the iMSTiTUiioRa akd CmuzA-
TION OF THS EaSTEKN CaLIPHATE.
Mohammed had begnn to bestowpolitical unity on Arabia;
bat he had done still more : he had given her the Koran,
as the starting-point and base of the futnre civilization ef
Islam. It was for the preservation and the better under-
standing of the sacred text that the first believers were
led to create grammar and lexicography, and to make col-
lections of the poems of their own and former times, those
" witnesses of the meaning of words," as the Arabs call
them. To elucidate questions of dogma they created
theology. Jurisprudence, in like manner, issued from the
Koran, and the historical sciences at first gathered around
it.; is early as the first century of the Flight, schools
w«e founded in Tri^:, at Basra and at Cufa, in which all
the "questions to which the study of the Koran gave rise
v^re stated, and answered in different ways. Natural
scknco and mathematics were less directly concerned with
the sacred book, and were consequently neglected during
the whole period of the Omayyad dynasty. They only
l>egan to be cultivated when, under the .'Abbfisids, the
study of philosophy led to the nse of translaticns from the.
Greek. The institutions of Islam were developed, no
doubt, ea new wants made themselves felt, in proportion
to the extension of the empire ; but they were nevertheless
founded on the Urst arrangements made by the Prophet,
and handed down by him in the Koran.
Under the first four Caliphs these institutions continued Political
in a rudimentary state. The Caliph {Khcdifcu, substitute.^*
or successor) was elected by the Moslem community ; i^jjiio.
and, after receiving from all its members the oath of tions.
fidelity {BaCa) which they were bound to take, united the
temporal and spiritual powers in his own hands. He T.as
at the same time high priest, ruler, .and judge. He was
compelled, however, by the very extent of tie empire to .
delegate his powers to those agents (^Amil, plural 'Ommdl)
whom he commissioned to represent him in the provinces.
The State revenues, which entered the public treasury
{JBaii al-mdi), were composed — (1) of the tithe, or tax for
the poor {Zakdt), which every Moslem was bound to pay ;
(2) of the fifth, raised on all booty taken in war, the rest
being divided among the warriors ; (3) of the poll-tax
{Jizya) and the land-tax {Khardj), which only affected non-
Moslem subjects. The Caliph administered the revenues
of the State at his own pleasure, applying them to the neces-
sities of war, to public works, to the payment of officials,
to the support of the poor, and to the distribution of the
annual pensions, in which every Moslem had originally
a right to share. The State could possess landed property.
Under "Omar I. we find that the pasture land belonging
to the State supported not less than forty thousand camels
and horses. To 'Omar L was due the regulation of the,
poU-tai by a fixed scale. The rich, whether Christians or
Jews, paid four dindrs (about thirty-two shillings) yearly ;
people of the middle class, two dinirs ; the poor, one
dlnir. Besides this payment in money, the subject-racea
had to make contributions in kind, intended for the
support of the troops. The land-tax consisted of a general
rent in proportion to the extent, character, and fertility of
the lands possessed by the conquered.
As the simis produced by these different imposts were Tt -.
often very considerable, it became necessary, as early as Cfv.io,'
the Caliphate of 'Omar L, to create a special office,
charged with the accounts of their expfcnditure. Its
organization was borrowed by 'Omar from the Persians,
and it retained its Persian name of Diw&n, a term after-
wards applied to all government offices. The Arabs at
that time being torf illiterate for such employment, the
task of keeping the registers of the Dlw4n was entrusted
to Greeks, Copts, and Persians. 'Omar also gave his
attention to the apportionment of the individual pensions
of the Faithful Every one received a larger or smaller
sum according to the greater or less nearness of his con-
nexion with the family, or the tribe, of the Prophet.
Thus 'Aisha, who had been the favourite wife of
Mohammed, received a yearly pension of twelve thousand
dirhems ; ' the other widows of the Prophet only received
ten thousand. The Hdshimites and Mottalibites, that is,
the members of the Prophet's family, also received ten
thousand dirhems. The Emigrants and the Defenders, or
those citizens of Mecca and Medina who had been the
first to embrace Islam, had fi^e thousand dirhems; and
that was the sum which "Omar L allotted to himself.'
For every other Moslem of fvdl age, the pension varied
from 4000 to 300 dirhems. We can easily understand
what an influence the hope of this pension must have
exerted on the conquered races, and how much it m\ist
' Tlie dirbem was equivalent to one franc.
' His moderation was not imitated ty bis soocessor O^min, wBB
made it bis principid object to enrich _^1 the iiiember^or.hu Ojta
family at tbe expense of tno rest p(,tbA.lIosleiii*,
590
M 0 H A M M E D A P^W S M
[ixsTiinnoKS
JlUitary
itistitu-
tiOQ!'
■Ccromc-
Hercdi
tory ^u
have contributed to their conversion. On accepting Islam
they acquired a right to tho pension, besides ceasing to pay
the land-til s and the poll-ta
Even in the earliest days of Islam the Arabs were not
entirely devoid of military skill. Many of their tribes
had been brought into relations with the Greeks and
Persians, and had acquired from them some ideas of tho
art of war. ThuSj in the time of Mohammad, the division
of an army into a centre, right and left wings, vanguard
and rearguard, was understood, and the art of defend-
ing a camp or a city by entrenchments was also known.
The Arabs fought on foot, on horseback, and moimted
on camoh. The arms of the- infantry con.=isted of a
spear, a sword, and a shield, and sometimes also of
a bow and arrows. The horsemen fought chiefly with
tho lance. For ■ defensive arms, besides the shield, the
Arabs were acquainted with the 'helmet, the coat of mail,
and the cuirass of leather covered with plates of iron.
It was not till the period of the Omayyads that they
began to employ military engines, such as the balista.
The array was divided by tribes; and each tribe had its
flag, wiiich consisted of a piece of cloth fastened to a
lance. As regards the recruitment of their armies, every
man able to carry arms was originally bound to render
military service. 'Omar I., to whom Islam owes so
many of its institutions, was the first to divide his
armies into distinct corps, and to assign to each corps a
fi.?ed station. Thcce stations were the province of Cufa,
that of Basra, and afterwards the provinces of Emesa, of
the Jordan, and of Palestine. These provinces afterwards
became military colonies, all the inhabitants of which were
bound to render military service, as distinguished from
tho other provinces, where service was optional, or at all
events regulated by the necessities of the moment.
With the accession of Mo'iwiya I. to the supremo power,
the mechanism of the State was modified and became more
eoaplipated. SIo'Awiya endeavoured to copy the cere-
monial of foreign courts. He built himself a palace at
Damascus, and set up a throne in the audience-chamber,
the door of which was kept by a chamberlain {H^(jib).
V/hen he attended tho service at the mosque, he occupied
a close pew with a grating in front {Makmra). When
ho left his palace, he was surrounded by a bodyguard
(Shorta), commanded by a provost {Sdhib al-Shortu). Lastly,
iTi his 0".ni lifetime, he caused his son Yazld to be acknow-
ledged as his heir-presumptive, and thus estabUshcd tho
principle of hereditary succession, which was opposed to
the spirit of Islam, and was the soiirce of every kind of
calamity. As regards the administration of the State,
Mo'i'iwiya acted at his own will and pleasure. Thus, in
order to secure tho services of 'Amr b. al-'As, the conqueror
of Egypt, ha gave up to him the revenues of that province,
a part of which ought to have gone to the State. He alio
to'ik an important step with regard to the annual pensions
of the Faithful, which he reduced by about two and a half
per cent. The administration of the public funds in the
diiTerent provinces v.'as left to their Prefects, who were
c.tpected to pay into the public treasury only the surplus
of their respective revenues. The empire had been at first
divided into ten provinces — 1. Syria (subdivided into four
Joyid, or military districts) ; 2. Cufa, ivith Arabian 'IrAlj
and Persian 'Irilj; 3. Easra, with Persia, Sijistin, Khorisin,
Bahrain, and 'Omin ; 4. Armenia ; 5. Mecca ; C. Medina ;
7. The Indian Marches ; 8. Africa ; 9. Egypt ; 10. Yemen.
Mo'dwiya, however, subsequently thought proper to make
IChorisAn a separata province. Under his successors, and
according to the necessities of the moment, it was some-
times reunited to the government of 'Irdk. In 'Irdlf itself,
Mo'.^wiya joined Basra and its dopend^encies to Cufa.
Under Mo'Aw;ya the Prefects had the most extensive
civil and military powers. They had even the right of tht
direct appointment of their Bub-Prefects. Mo'awiya, nob
vnthstanding, thought it advisable to disconnect fron
their pnivers tho offices of Judge (Kddi) and of P.eligioa
Oificial {Im&ni), which were entrusted to special function-
aries named directly by the Caliph. The Caliph waa,
however, always at liberty to modify these arrangements at
his own pleasure. Under the successors of Mo'dwiya, wo
find certain Prefects invested at the same time "With the
dignities of Cadi and Imdm.
It -n-as also to Mo'dwiya that tlie State owed the creation Caan
of a Chancery (Dlyvin al-akhtdm, or Seals-ofiice), in which cc.7.
all decrees proceeding from the Caliph were registered ; so
that, when once issued, these decrees could not be falsified
Mo'dwiya also exerted himself to ensure rapidity of com- Tosti.
munication throughout the empire, by instituting the
courier-post (Sarid), in imitation of the post of the
Persians and Byzantines.
After Mo'dwiya we must come down to the time of
'Abd al-Melik to meet with any important innovations in
Moslem institutions. Before the reign cf that Caliph
the books of the public offices were kept by Ciiistians
and Persians, and drawn up in Greek and Persian. 'Abd
al-Melik ordered the exclusive employment cf the Arabic
language, and substituted Moslems for aU. the Christian
and Persian clerks in the government offices. It was this
same Caliph who founded the monetary system of Islam, Jloney
and who was the first to strike dindrs (pieces of gold
worth about ten francs), and dirhcms (pieces of silver
worth about a franc), with legends in Arabic. The
postal .system was also very much improved and developed
under this prince. 'Abd al-Melik v. as powerfully seconded
by the famous Ilajjdj, who was able to re-establish in
'Irdk the disputed principle of obligatory military service,
and who also succeeded, by skilful management, in raising
tho condition of agriculture in that province. Walld, the
successor of 'Abd al-Melik,, especiallj' distinguished himself
by the foundation of religious institutions. In his reign RcHgioa
the mosque of Damascus, half of which had hitherto f^'--»-
remained in the hands of the Christians, was appropriated '■"'''^
exclusively to the Moslems, and considerably embellished.
Hospitals were also established for lepers, the poor, the
blind, and the sick. The pious 'Omar H. devoted all his
efforts to the embellishment of the mosque of Damascus.
An edict of 'Omar I. had forbidden Moslems to acquire
landed pro])erty, agriculture being considered an occupa-
tion unworthy of a free man. This law had fallen into
disuse ; but "Omar H. put it in force again, and declared
null and void every purchase of land made ty a Moslem
subsequently to a.h. 100. The effects of this law might
havo been fatal to the empire ; but . it again became
obsolete imder tho Caliphate of Hishdm.
At the accession of the 'Abbdsids the centre of tho 'nstt'.-.
empire was displaced. Damascus fell from the ranlc of|^°°' ,
its capital to that of a provincial town ; while Baghddd, '^j,";""'
a spall and unknown village, became the mistress of tho r,is.
world. Under the first 'Abbdsid the empire — not includ-
ing the province of Baghddd — was divided as follows : —
1. The province of Cufa ; 2. The province of Basra, with the
district of tho Tigris, Bahrain and 'Omdn ; 3. Hijdz and
Yamaraa; 4. Yemen; 5. Ahv.dz; C. F.drsistdn; 7. IChordsdn;
8. Tho province of Mosul ; 9. Mesopotamia, with Armenia
and AzerbaijAn ; 10. Syria; 11. Egypt and tha province
of Africa (Spain being a dependency of Africa) ; 1 2. Bind.
Al-Safi"d:.i afterwards made Palestine a distinct province,
and separated Armenia and AzerbaijAn from Mesopotamia.
Still later, Hdriin al-Kashid created a new province to tho
north of Syria, which received the name of 'Awdsim. Each
newly-conquered province was always united to that ono
of tho older provinces to which it was nearest.
SNSTITUTlOIfS.]
MOHAMMEDANISM
591
Piime
Minister,
_A(Jmini3-
trftti'e
■aoTTtcej.
drgani-
Eation of
theStete.
SUiph.
Minis
'ton.
Simultaneously with the accession of the 'Abbisids,
Persian iBfluence began to preponderate. The Persian,
Eh^lid b. Barmak, was entrusted with the administration
of the finances (Diwdn al-E/tardf) by As-Saffiih, who was
.also the first Caliph who transferred the burden of public
affairs from himself to a Prime Minister ( WaAr, whence,
in European languages, the term Viiier). The title of
•Wazlr was unknown to the Omayyads. The office of
Prime Minister was of Persian origin. It existed till the
time of the Caliph Kidl, when that of Amir al-0mar4
•was substituted for it. When the Caliphs had fallen
under the tutelage of the Biiyids, it was the latter who
chose Viziers, leaving to the Caliphs only Secretaries
{Rajfis al-Ruwasd). Under the Seljillj: Sultans the Caliphs
■were again permitted to choose their own Viziers.
The institution of the office of Vizier was not the feast
among the causes of the decadence of the Eastern Caliphate.
The 'Abbisids gradually became unaccustomed to the
exercise of power and the management of affairs, and thus
lost all direct influence over-their subjects. Besides the
Minister of Finance and the Vizier, the 'Abbisids created
another important office, that of Postmaster-General {Sdh,ib
alrBarii), whose duty it was to collect at a central office
all the information which arrived, from the provinces, and
to transmit it to the Prime Minister. Thus the adminis-
trative services were greatly lartended under the 'AbbAsids.
They were subdivided as follows: — 1. Diwdn dl-Khardj, or
Ministry of Finance; 2. Diwdn al-DiyS, or Bureau of
State property; 3. Diwdn al-Zimdm, Registry Office or
Exchequer Office ; 4. Diwdn al-Jond, or Ministry of War ;
5. Nazar al-Mazdlim, or Court of Appeal ; 6. Diwdn cU-
Mawdli wal-GhUmdn, or Bureau of the freedmen and slaves
of the Caliphs ; 7. Diwdn Zimdm al-Nafakdt, or Office of
Expenditure ; 8. Diwdn aUBarid, or Office of the Posts ;
9. Dividn cd-RasdU, or Office of Correspondence; 10.
Diwdn al^Taukt, or Office of the Imperial Seal, and of the
registration of official documents. There were also offices
for the despatch and reception of official dociunents, and
for the inspection of weights and measures.
We cannot better conclude this brief stimmary of the
institutions of the Caliphate than by giving a sketch of
the organization of the State, according to the Moslem
authors themselves.
The supreme chief received the title of Caliph, or of
Commander of the Faithful (Amir al-Mo'minin). He
united in his own person all the powers of the State ; his
Ministers and all public functionaries acted only by virtue
of a commission from him. They, like all other Moslems,
were at the mercy of the Caliph, who had power of life
and death over them. As spiritual chief, the Caliph was
also the supreme judge in questions of dogma. In theoi-y
he held his powers by the free choice of the majority of
SToslcms; but, when he had once received their oath of
allegiance, he became their absolute master. The first
condition of eligibility to the Caliphate was to belong to
the tribe of Koraish. In Moslem belief, the subjects of
the Caliph owed him obedience and aid so long as he
should fulfil his duties with exactness. These consisted
in maintaining the principles of religion, in administering
justice scrupulously, in defending the territory and assur-
ing its safety, in carrying on war for the subjugation
of the infidels, and in spending the public revenue in
conformity to the law. If the Caliph failed in the
performance of his duty, rebeUion against him became
lawful.
The ilinisters might be absolute or dependent. ' If
dependent, they simply executed the orders of their
sovereign. If absolute, they took his place, and exercised
all the powers of a Caliph except that they could not, at
least in tbeotj, designate any suoceasor to the reigning
Galipn. It was only to the Caliph himself that they were
responsible for their actions.
The Prefects, when once appointed, whether by thePi«feeB
Caliph or the Vizier, became so many petty sovereign.i,
and, legally, owed an account of their actions .only to the
Caliph, or to his Prime Minister, when the latter was
absolute.
The Generals were appointed either by the Caliph or by Oena
the Vizier, or lastly by the Prefect, when only a local war ^'^
was iu question. They were sometimes invested with
very extensive powers, such as those of concluding treaties
of peace, of administering justice, and of dividing the
booty. The General, in his- turn, appointed the officers
{Kakihs) and under-officers I^Arifs). It was a general
order that infidels, before hostilities against them were
opened, should be summoned to embrace the faith, or to
submit by capitulation. The conversion of infidels was
valid, even when effected sword in hand, on the field of
battle, and the new convert became inviolable in person
and property. On the other hand, every infidel taken
prisoner was sold a^ a slave, with his wife and children.
He might even be put to death. Apostates were never to
be spared ; they were put to death, and their property
confiscated.
Justice was administered by Cadis, appointed eitner by Cidis.
the Caliph, by the Vizier, or by the Prefect. To be eligible
as a Caxli (Kddi), it was requisite that a man should
be — 1. A male and of respectable age ; 2. In full pos-
session of his mental and physical faculties ; 3. A free
man ; 4. A Moslem ; 5. Of good moral character ;
6. Acquainted with the principles of the law and their
application. The duties of the Cadi were to examine into
the disputes and lawsuits brought before him ; to enforce
the execution of his judgments; to name judicial councils
for the administration of the goods of minors, madmen,
etc.; to administer the mortmain property of mosques and
schools (wakf, plural woku/) ; to watch over the execution
of wills ; to inflict due legal penalties on those guilty of
crimes or misdemeanours ; ' and to inspect the highways
and public buildings. When any locality possessed no
Imim, or public officiator at the mosque, it was the Cadi
who performed this duty. The assistants of the Cadi
were Notaries (Shohud), Secretaries (Omand), and Deputies
(Ndyibin). If the Cadi died, his subordinates lost their
offices ipso facto. On the other hand, the death of a
Caliph did not nullify the powers of the Cadi ; but it was
necessary that he should be confirmed by the new sove-
reign.
The Court of Appeal (Ifazar al-Mazdlim) was instituted Cr.iH of
to take cognizance of those causes in which the parties ■'■ IT"'-
concerned appealed from the judgment of the Cadi. The
sittings of this court were presided over by the Caliph in
person. It was established by the Omayjad 'Abd al-Melik.
The last Caliph who sat in public to examine appeal cases
was Mohtadi. After him a special judge v/as appointed to
the function of presideiit of the Court of Appeal.
Besides the Judges there were Inspectors (Mohtasib), I.-^pw
charged with the police of the markets and the care of '^-"^
morals. The Mohtasib's duty was to take care that
weights and measures were not falsified, and that buyers
were not deceived as to the quality of the goods sold. He
had the power of inflicting summaiy punishment on delin-
quents, but only in the case of flagrant offences. If the
person charged denied the facts, he was to be brought
before the Cadi As regards morals, the Mohtasib took
care that widows and divorced women should not remarry
befbre the expiration of the legal period prescribed by. the
' The principal offences werev-apostasy, neglect of religions duties,
refusal to pay tazea, theft, adultery, outrages, and murder. The
penaltiu were impriaoBment, fiaea, corporal puimhmest, and death.
592
MOHAMMEDANISM
[thxoloot?
Marsha
of the
Koran. Slares and beast's of burden were placed under
his guardianship, and he protected them from ill-treatment
on the part of their masters. The Mohtasib was also
commissioned to prevent public 8candal.% such as the sale
of wine ; to forbid Christians and Jews from building
houses higher than those of the Faithful ; and to enforce
their wearing on their dress a distinctive mark (Ghiydr).
Besides the offices already described, there existed three
others which require mention — those of the Marshals of
the Nobility {NiJcdbat al-Ashrdf), of the ImAms, and of the
Emirs of the Pilgrimage.
The Marshals of the Nobility were appointed in the
different provinces either by the Caliph, by his represent-
Nobility. ^(^j^gj^ or by the Grand Marshal. Their functions were
to superintend the descendants of the family of the
Prophet, who formed the nolsility of Islam, and to keep a
register of all the births cfnd deaths which occurred in the
families of the members of this nobility. In every pro-
vince there were two Marshals, one for the family of 'AU,
the other for the 'Abbisids.
I'Diw. The duty of the Imim was to recite the publio prayers
in the mosque. He was appointed by the Caliph or his
representatives, and chose in his turn his Mo'edhdMna,
who called the Faithful to prayer from the tops of the
minarets. In the Friday prayers it was the duty of the
ImAm to invoke p\iblicly the blessings of Heaven on the
reigning Caliph.
Leader r.f The leadership of the yearly pilgrimage to the temple
ihe H\ij. of Mecca was considered a great honour. It was almost
always the Caliph himself or one of his near relatives who
assumed the function of Amir al-Hajj. The duties of this
teader of the pilgrimage were — 1. To escort the pilgrims in
safety on their journeys to Mecca and back ; 2. To direct
the religious ceremonies during the 6ojoui-n of the pilgrims
at the Holy City.
Such, briefly stated, was the organization of the Moslem
State. Let us now say a few words on its religion.
Kelierion. We need not now recur to the subject of the doctrines
of Mohammed, which are treated of in their own place ;
but it is imixirtant to show what they became after the
time of the Prophet, and what movements they aroused
in Islam. The diversity of the conquered races was of
itself sufficient to introduce, in the course of ages, serious
modifications of the earlier religion.
But, from the very first, the Koran contained wathin
itself the germs of discord. As long as men were content
to adopt its teachings without discussion, orth jdoiy might
boast of maintaining Itself unbroken. But a/ soon as they
Bought to examine deeply into its meani ig, dilficultiej
arose, which necessarily led the strongi.st mind' into
doubt and uncertainty. In jjarticular, the conception of
God, predestination, and free-will, as preseiited by the
Koran, could not bear examination. As early as the fii-st
century of the Flight a theological school was founded nt
Basra, the most renowned master of which, Hasan al-
<»:;i,l Basri, introduced the critical study of dogmas. His dis-
Mu.;/ .if ciplesj who were for the most part Persians, could not fail
soon to discover that the Koran often contradicted itself,
and especially that it left many dogmatic difficulties unre-
solved. One of the disciples of Masan, WA-sil b. 'Ati, set
forth his scruples publicly, departing on three points from
the orthodox doctrine. The Koran affirms the attributes
of God ; W.lsil b. 'At4 denied them ; because^ he says, if
the attributes of God arc eternal, they constitute in some
sort so many deities. Wo ought not therefore to affirm
the existence of an attribute — that of justice, for example
— but simply to affirm that God is essentially just. The
Koran admits the doctrine of predestination ; Wisil
rejected it, as incompatible with the theory of rewards
and punJ.shmont3 in another life, which presumes absolute
free-will m man. The Koran epeaka only of paraaise &Bck
hell ; Wisil admitted a purgatory. The sect founded by'
Wisil received the name of Mo'tazilita (dissident), or Mo'tait"
Kadarite, that is to say, which recognires in mau a power ''!'"■
(A'acAar) over his own actions. Another sect, that of the
Jabarites (Partisans of constraint) agreed with the Mo'taii- JtW
lites on the question of the attributes, but were diametri- "l**-
cally opposed to them on that of free-will; The Jabarites
denied to man the slightest share in his own actions, and
believed the very smallest actions of men to be the effect
of predestination. The Koran, not concerning itself with
the contradiction involved, admits at the same time the
responsibility of man and the absolute predestination of
his actions. The Jabarites rejected all responsibility, and
believed that man is predestined from all eternity to para-
dise or to hell, for no other reason than that God has so _
willed it. A third sect, that of the §ifatites (Partisans of a£»tfte«
the Attributes), contended energetically against the two
former. Keeping to the t«xt of tho sacred book, they
alleged, for example, that when it is said in the Koran,
that God is seated on his throne, the expression must bo
taken literally. They thus fell into the grossest anthropo-
morphism, a doctrinfe which was very far from the ideas of
Mohammed. In the face of these heterodox sects, tie
orthodox made but a poor figure. Eejecting, in their
commentaries on the Koran, the explanations alike of the
Mo'tazilites, of the Jabarites, ■" and of the Sifatitea, but
acknowledging their • inability to refute them systemati-
cally, they merely opposed to them a declaration that tha
Koran was neither to be explained aUegoricallj'nor always
taken literally ; and they concluded that, where two con-
tradictory expressions could not be reconciled, a mystery
must be admitted to exist, which it would be vain to
attempt to fathom. But they did not always keep within
thja limits of discussion. Under the reign of 'Abd al-
Melik they succeeded in bringing about a persecution of
the sectaries.
The Jlo'tazilites, the Jabarites, and the gifatites were
dangerous only to tho Church. Other sects arose, which
put the State itself in peril It will be remembered that,
at the time of the dispute between "AU and Mo'Awiya,
twelve thousand of the partisans of the former deserted
him. These revolters, or Khirijites, originated one of the Khir-
most formidable sects which ever existed in Islam. TheJ''"-
KhArijites rejected in principle the Caliphate and the
Imimate. At all events, they did not acknowledge the
exclusive right of the Koraish to the Caliphate, but
declared that, if it was absolutely necessary to elect a
Caliph, his origin was of little consequence, provided he
fulfilled his duties conscientiously and exactly. We have
seen for what a length of time they kept the Omayyads
in check. AVben they had been put down in Asia, they
passed into Africa, and there made numerous proselytes
among the Berbers, disposed as these were, by their
independent character, to adopt with enthusiasm the
principle of anordiy. The most terrible, however, of the
militant sects which were formed in the bosom of Islam
was that of the Shl'itcs. Originally the ShTites wereShi'ittc
simply the partisans of 'All and of his descendants. In
the course of time, when the whole of Persia had adopted
the cause of the family of "Ali, Shl'ism became the recep-
tacle of all the religious ideas of tho Persians, and Dualism,
Gnosticism, and Slapicheisin, were to be seen reflected in
it. Even in the lifetime of 'AH, a converted Jew, named
"Abdallih b. SabA, had striwn to introduce foreign
elements into Islam. Thus, ho alleged t)ir.t 'All was to be
adored as an incarnation of the Deity. These ideas,
though rejected witli horror by 'AU himsJ/, and by the
greater part of the first Shi'itt.s, gr.idually ma.' ■ way ; and
aU the direct descendants of 'Mi became veritavic deities in
OEcrs.]
MOHAMMEDANISM
593
Ths
ortho-
dox
•ect3.
the eyes of their respective partisans. " K further distinc-
tion between the SWites and other sects is, that they
introdaced the practice of giving the Koran an allegorical
interpretation. Tiiis system permitted them to see in the
Bacred book whatever meaning they chose, and was carried
out at a later date, as we shall see, by the founder of the
Ismailian sect.
Under the "Abbisids it seemed for a moment that the
Shi'ite doctrines were about to triiunph. We know, in
fact, that the foftnder of that dynasty gave himself out as
the heir of the house of 'Alt. But reasons of State
prevailed, and the 'Abbisids, false to their first professions,
on the whole supported orthodoxy. Under their reign
were established the four orthodox sects — MAIikite,
Hanafite, Shdfi'ite, and Hanbalite, which even at this day
divide between them the whole Moslem world. They are
named after their f oiinders — MAlik, Abu Hanlfa, Shdfi'i, and
Ibn Hanbal. These sects only difi'er from each other on a
few points of civil and religious jurisprudence. They agree
on questions Of dogma. It was not, however, without
difficulty that orthodoxy succeeded in obtaining the
victory. Under Ma'miin and other Caliphs several doctors,
as we have seen, were persecuted for believing that the
Koran was the uncreated word of God. From the time
of Motawakkil, however, -orthodoxy regained the upper
hand. Still, this reaction would not have lasted long, in
face of the advance in science which marked the accession
of ila'mun to power, if the orthodox had had no other
defensive weapons than material force and the assent of
the majority. As philosophy made its way La Islam,
thanks to the translations from Greek authors, which
were made principally during the Caliphate of Ma'mto, it
called forth in men's minds a movement of scientific curiosity
which might have been fatal to orthodoxy. In the tenth
century of our era a society of encyclopedists was formed at
Ba- ra, who, under the name of Ikhwdn al-Saf A, or Brothers of
Purity, put forth a number of very ciirioua treatises, in
which all sorts of physical and metaphysical questions were
discussed and resolved in a scientific manner.* There is no
doubt that these lucid and attractive writings would have
led to a great religious revolution, if the orthodox had not
understood the danger of their position, and applied
themselves also to the study of philosophy, for the pur-
pose of employing it in the service of the faith. It was
thus that, towards the middle of the tenth century, a
certain Abii '1- Hasan al-Ash"arl, a descendant of that Abii
Jjii'al. MiisA al-Ash'arl who had formerly acted the part of
arbitrator in the dispute between Mo'dwiya and 'AU,
struck out a S3'stem in which religion appesued to be
reconciled with philosophy; a system which was natur-
ally sure to attract all commonplace minds — that is to say,
the greater number. Ash'arism, or philosophic theology
(KalAm), was adopted with enthusiasm by the triumphant
orthodox doctors, and thenceforth pure philosophy and the
heterodox sects ceased to extend their influence."
The creation, however, of this philosophical theology
had not done away with aU dangers for orthodoxy. We
have seen above that the Shfa/ were divided into several
sects, each holding for one of the direct descendants of
'Mi, and paying him the reverence due to a deity. One of
these sects, called the Ismailian, because it acknowledged
Ism.-i'll, the seventh Imiim or Pontiff of the jjostcrity of
'jUf, as its chief, was the source of the greatest disorders
in the Moslem empire, and was not far from being
triumphant in Asia, as it was for a long time in Egypt.
The Ismailians, like all the other Shl'ites, believed in the
Tsmai li-
ana.
' The most important have been translated into German by Prof.
Dieterici,
^ See Houtsma, Ds Strijd over hei dogm/i in den Isldm tot op el-
Aah'ari; and Spitto, Zkt QescMchte Aia'l-^asan ai-Aiari'a.
coming of a Messiah, whom they called the Mahdl,- and
who, according to them, was one day to appear on earth,
in order to establish the reign of justice and equity, and
to take vengeance on the oppressors of the family of 'All.
They also believed in a God of far more elevated character
than the God of the Koran, one who was unapproachable
by human reason, and who had created the universe, not
directly, but by the intermediate action of a sublime
being, the .Universal Reason, produced by an act of God's
will. The Universal Reason, in its turn, had produced
the Universal Soul, which, on its part, had given birth to
primitive Matter, to Space, and to Time. These five
principles were the causes of the imiverss. Man, emanating
from them, ha.d a tendency to reascend towards his source.
The chief end of his being was to attain to perfect union
with the Universal Reason.^ But, left to himself, man
would have been powerless to attain this end. The
Universal Reason and the Universal Soul therefore became
incarnate among men, in order to guide them towards
the Ught. These incarnations were no other than the
prophets in all ages, and, in the last period, the Imilms of
the posterity of 'All. In the second half of the ninth
century, a Persian, bom in Susiana and named 'AbdallAh
b. Maimun al-KaddAh, nourished the dream of destroying
Islam, and thought these doctrines, suitably modiied,
likely to be highly usefid in carrying out his purpose.
He devised a system at once religious, philosophical,
political, and social, in which, as he thought, all beliefs
were to meet and mingle, but^and in this consisted its
originahty^-a system so graduated to suit different
degrees of intelligence, that the- whole world should
become one vast Masonic association. The chief of the
Ismailians, the ImAm lomu'll, having died, 'AbdallAh
asserted that his son Mohammed b. IsmS'il was to succeed
him as the founder of this new religion, which it was
'Abdalldh's mission to announce to the world. Since the
creation of the world, as 'AbdaUdh assorted, there had
been six religious periods, each marked by an incarnation
of the . Universal Reason in the person of a prophet.
Adam, Noah, Abraham, Jfoses, Jesus, and Mohanix.ed
had been the prophets of these periods. Their mission had
been to invite men to accept more and more perfect forms
of religion. The seventh and last religion, and the most
perfect of all, was that of .Mohammed b. Ism&'il, the true
Messiah. The IsmaiUans, as may be imagined, readily
embraced the theories of 'AbdallAh. In addressing other
sects and religions, 'Abdall.'lh used special arguments
with each. With the philosophers he dwelt on the
philosophical principles of his doctrine. The conversion
of Christians, Moslems, or Jews, was a more difficult
task. 'AbdaUAh had established several degrees of initia-
tion, and it was only by slow degrees, and with the most
minute precautions, that he gained a mastery over the
mind of the future proselyte. His curiosity was first
aroused by allegorical interpretations of the Old Testament,
the Gospels, and the Koran, ajd by proposing to him reli-
gious problems which could not be solved by any of the
existing religions. The solution of these problems was not
to be given to him till he should have signed a compact,
and sworn Aever to reveal the mysteries with which ha
was made acquainted. If he took this pledge, he thence-
forward belonged, iDody and soul, to the sect ; and woe to
him if he made any attempt to -svithdraw himself from the
authority of his chiefs ! The compact signed, the newly-
initiated disciple had to make a certain payment, which
went to swell the treasury of the sect. The secret society
* It need hardJy be said that all these doctrines were borrowed
fiom Gnosticism and from Xeo-Platonism. See on the Ismailian sect
Guyard, Fragments rdalifs d la doctrin" dcs Tsma^liens, and Cn^prand"
mallre dcs Assassins au temps de Saladin, "^
594
MOHAMMEDANISM
[law."
four.Jed by 'Abdalldh soon had a great number of mem-
bers, and its missionaries spread themselves over the
Jloslera world. Towards 887 a.d. an Ismailian, Kamddn,
surnaraed Karmat, founded the branch sect of the Carma-
thians, whose exploits have been recorded above. The
Ismailian preachers also made numerous proselytes in
Africa and in Egypt; and in a.d. 909, 'Obaid AllAh, a
descendant of the founder of the sect, but who passed as a
member of the family of 'All, founded the FAtimite dynasty.
Fit." Under the Fitimite Caliph Hikim, a new religion sprang
pites. out of Ismailism, that of the Druses, so called from its
inventor, a certain Darazi or Dorzl. This religion differs
little from Ismailism, except that it introduces the dogma of
the incarnation of God himself on earth, under the form of
the Caliph H4kim. This heresy did not survive (he reign of
lIAkim in Egypt. When the FAtimite Caliph Mostansir
ascended the throne, he re-established the Ismailian belief ;
and the Druses, driven from Egypt, took refuge in the
Lebanon, where they stiU exist. As for the Egyptian
Ismailians, they disappeared at the time of the conqiiest
of that province by the pious and orthodox Ayyiibite
Saladin. This, however, was not a final deliverance of
Islam from that formidable heresy. A hundred years
Iiefore the return of Egypt to orthodoxy, a Persian named
Hasan SabbAh, who had been initiated into Ismailism
at Cairo, in the household of the Caliph Mostansir, had
founded at Alamut, on the southern shores of the Caspian
Sea, that Persian branch of the Ismailians known to all
Airis- the world under the name of the Assassins,^ who held in
siii* check the most powerful princes of Islam, till they were
destroyed by the Mongol invasion. From Persia, Hasan
SabbAh succeeded in filling Syria with his Assassins, and
every one knows the part they played during the Crusades.
The Assassins of Syria have never entirely disappeared.
Even at this day some are to be found in the Lebanon.
There are also some representatives of the sect in Persia,
in India, and even in Zanzibar ; but since the 1 3th century
they have become completely inoffensive.
To conclude this sketch of the development of religious
beliefs, it remains to say a few words on one of the most
remarkable manifestations of Islam — its mysticism, or
Siifism. S^lfisni. In principle, mysticism is rather a mode of
j iractising religion than a distinct religion ; it depends on
the character of the believer's mind, and adapts itself to
all dogmas.^ It is the especial tendency of tender and
dreamy spirits. Thus among the Moslems it is a woman
v.'ho is considered to have founded mysticism. This woman,
named Rabl'a, lived in the first century of the Hijra, and
was buried at Jerusalem. Her doctrine was simply the
theory of Divine love. She taught that God must be
loved above all things, because he alono is worthy of !c ve ;
and that everything hero below must bo sacrificed in the
hope of one day attaining to union with God. These
views were too similar to the Neo-Platonic ideas respecting
the union of the human intellect with the Universal Reason
not to have an attraction for the Gnostics, who abounded
in the Shl'ito sects. Mysticism therefore made great pro-
jrrcss in Persia, and assumed the character of a sect towards
the year 200 of the Flight. A certain Abd Sa'id b. Abi '1-
]\liair was the first who advised his disciples to forsake
tlio world and embrace a monastic life, in order to devote
themselves exclusively to meditation and contemplation ;
a practice which may very jirobably have boon borrowed
from India. The disciples of Abii Sa'ld wore a garment
of wool (■?(?/), whence they received the name of fjufis.
J:!i'ifism spread more and more in Persia, and was enthusi-
astically embraced by tho.se who wished to give themselves
up undisturbed to philosophical speculation. Thus, under
the colour of Sufism, opinions entirely subversive of tho
faith of Islam were professed. In its first form §ufism
was quite compatible with Moslem dogma. It was satis-
fied to profess a contempt for life, and an exclusive love of
God, and to extol ascetic practices, as the fittest means of
procuring those states of ecstasy during which the sokJ was
supposed to contemplate the Supreme Being face to face.
But by degrees, thanks to the adepts whom it drew front
tho ranks of heterodoxy, ^lifism departed from its original
purpose, and entered on discussions respecting the Divine'
nature, which in some cases finally led to Pantheism.
The principal argument of these Pantheistic Siifis was that
God being one, the creation must make a part of his
being ; since otherwise it would exist externally to him,
and would form a principle distinct from him ; which
would be equivalent to looking on the universe as a deity
opposed to God. In the reign of Moktadir, a Persian Siifi
named HallAj, who taught pubUcly that eveiy man ij God,
was tortured and put to death. After this the Sufis showed
more caution, and veiled their teachings under oratorical
phrases. Moreover, it was not all the Sufis who pushed
logical results so far as to assert that man is God. They
maintained that God is all, but not that all is God. Siifism
exists in Persia even in our own day.
It has been explained that, imder the 'Abbisids, foui' i-<i»)
orthodox sects were established, aiid that these secta
difl'ered among themselves principally with regard to juris-
prudence. The law of Islam is one of its most original
creations, and can Only be compared in history with the
development of Roman law. The laws laid down by
Mohammed in the Koran might suffice for the Arabs as
long as they were confined within the bounds of their
peninsula. When their empire was extended beyond theso
limits, it was inevitable that this first code should becomo
insufficient for their wants. As early as the time of tho
first four Caliphs it was necessai-y, in giving judgment
on the new cases which presented themselves, to have re-
course to analogy, and to draw inspiration from decision>i
given by Mohammed, but not recorded in the Koran. Tho
.first fountains, therefore, of law were, besides the sacred
book, the traditions of Mohammed, or Hadith, the collective '''"'"'^^
body of which constitutes the Sunna, or custom. Theso • *•""•
traditions were for a long time preserved only in tho
memory of the companions of Mohammed, and of those to
whom they had been orally communicated. But at tho
beginning of the second century of the Flight tho need
was felt of fixing tradition in writing; and it was at
Medina that tho first collection of them was made. It
was due to tho jurisconsult JIAlik b. Anas. He rejected M.ilik
from his collection with the greatest care all traditions "'^^' .
which appeared doubtful, and only preserved about seven- ji^u,^
teen hundred, which he arranged in the order of their
subjects. To this collection he gave the name of ifouaUa,
or Beaten Path.^ After him came tho celebrated Bokhiri,
tho compiler of the Sahih,* in which he brought together
about seven thousand tradition.?, carefidly chosen. Tho
(fah'ih has continued to bo tho standard work on the subject
of tradition,
Tho traditions did not always supply the means of
deciding difficult causes. Tho first four Caliphs were
often obliged to have recourse to their own judgment in
the admirustration of justice. Their decisions {'Al/idr)J^"
were also collected at Medina, and helped to swell the Auiir.
store of juridical matter.
^ From Ila^hish'in, or caters of llashiah — that is, Cannabis Imlica,
' See Gu'ytini, " 'Abd ar-Kazzik ot son traiti do la priSdestination et
du libre arbitrt," Jmm. askit., Feb.-Mar. 1873 ; Dozy, Hct hlamimrj,
.2a cd. 13S0.
» Publislied at Tunis, in India, and at Cairo, i.H. 1280, Mritli tlio
commentary of Zarlxdnt.
* Krehl's edition' (Lcydon) is slill unfini^llc,1. Aa edition, fully
vocalised, iu 8 vols., appeared at T3ulak, A.U. 1296.
UTERATIIBB.]
MOHAMMEDANISM
595
flchoclof In 1r4? another school of law was formed, which is
liik. distinguished from that of Medina by a greater dfegree of
independence. While the lawyers of Medina held strictly
to the Koran, the traditions of the Prophet, and the
'Athir, those of 'Irife admitted, in addition to these, the
deductive or analogical method (Kiyds), according to
irhich it was lawful to create precedents, provided there
was no departiire from the spirit of the sacred book, from
the traditions of the Prophet, or from the corresponding
decisions of the first four Caliphs. Ibn Abi Laila, who
filled the oflBce of judge in 'Ird^ vmder the caliphate
of Mansiir, was one of the first to apply this system.
His renown, however, was eclipsed by that of his con-
temporary Abii Hanifa, who worked out a complete system
of jurisprudence, with which his name has continued to
be connected (Hanifite law). Fifty years after the death
of Abii Hanifa, Sh4fi% a pupil of MAlik, appeared at
Baghdad, and founded in his turn an intermediate system,
in which he endeavoured to hold an equed balance be-
tween the purely traditional and the deductive methods.
The fourth system reputed orthodox is that of. Ibn Hanbal,
a pupil of Shdfi'l. Ibn Hanbal strove above all things to
bring back religious observances to their primitive purity.
Hi", doctrine was a kind of puritanism. As may be sup-
posed, each of these systems has been subsequently deve-
loped and commented on in a multitude of works, even
the names of which it is impossible to enumerate. In
order, however, to give some idea .of what a Moslem
treatise on jurisprudence is, we shall point out the principal
subjects contained in it. It treaU successively — 1. Of.
Purification (ablutions commanded by the law, purification
of women, circumcision, etc.) ; 2. Of Prayer as commanded
by the law ; 3. Of Funerals ; 4. Of Tithe and Almsgiving ;
5. Of the legal Fast ; 6. Of the Pilgrimage to Mecca ; 7.
Of Commercial and other transactions ; 8, Of Inheritance ;
9. Of Marriage and Divorce ; 10; Of the Faith ; 11. Of
Crimes arid Misdemeanours ; 12. Of Justice ; 13. Of the
Im.^mate or spiritual power, and of the Caliphate or tem-
poral power. It is thus a complete code, religious, civil,
penal, and governmental, that Moslem treatises on juris-
prudence set before us ; a code which embraces and foresees
all the circumstances both of public and private life.
The development of science and literature runs parallel
with the development of law. Before the time of
Mohammed the Arabs had been distinguished oidy by
ft rare poetical talent. Islam was the signal for the
Bpringing up of all the sciences and of literature. While
the study of the dogmas and ordinances of the Koran
was producing theology and jurisprudence, the necessity
of preserving the exact text of the sacred book, and of
teaching the new converts the language of the Prophet,
was giving birth to grammar and lexicography. The first
school of grammar was established at Ba.sra. The first
attempts at grammar are generally attributed to a certain
Abii '1-Aswad al-Do'ali, who was tutor to the children of
Ziy.W, the brother of Mo'Awiya. According, however,
to some authors, the honour of having discovered the
first elements of grammar ought to be attributed to a
Persian, named 'Abd al-Rahm4n b. Hormilz. Be this as
it may, a foreign influence must be recognized at the
very commencement of this science. The vowel marks,
for instance, were imitated from those of the Syriac. The
division of the parts of speech into noun.?, verbs, and
particles was indirectly borrowed from Greek grammar.
Yet the Moslems, once in possession of the principles of
grammar, knew how to develop and apply them in an
admirable manner. A perfect galaxy of grammarians
arose in the track of Abii '1-Aswad ; a rival school to that
of Basra was established at Cufa, and grammar r.ttained
its highest degree of perfection imdsr the first 'AbDAsids ;
Scieno
and
letters.
as is shown by the voluminous treatise of SfbSwaihi, known
under the name of Kitdb,^ or the Book par excellence.
In lexicography, the Arabs were at first content to ex-Lexko-
plain the rarer words of the Koran, of the traditions, and g™p!>;-
of the ancient poems ; and to collect lists of terms applying
to the same object, as the camel, the horse, the sword, etc.
Thus small coUections were formed, which served afterwaids
for the composition of dictionaries. The first dictionary
properly so called, composed in Arabic, appears to have
been the Kitdb al-^Ain of Khahl b. Ahmed al-Far4hidl, a
contemporary of H4r\in al-Rashid. After him came Jauharl,
■whosB.Sahdh may still be consulted with profit. The cele-
brated Zamakhsharl composed a dictionary of metaphors
imder the title of Asds al-Baldgka. Lastly, Tha'ilibl, in
the 11th century of our era, drew up his Fikh al-Logha*
a work specially devoted to synonyms. The accessory
branches of jihilology gave occasion to some important
worka. The ancient poems and proverbs were collected
and commented on. Thus Ab>i TammAm formed his Antho-
logy, called Hamas A (q.v.), and MaidAni his collection of
proverbs {Kitdb amthAl al-'Arab).^ The study of poetry. Poetry
with special regard to its rhythm, led Khalll b. Ahmed, ""^ -^ ■
already mentioned as a grammarian and lexicographer, to ""•"'-'^
the conception of prosody. He wrote the first treatise on
that science, which served as a model to all subsequent
writers on metre.* Pure literature remained confined to
poetry. It was not that the Arabs were without any
conception of the romance, the tale, or the novel. The
adventures of Antar, the romances of Dhii '1-Himma and
of Saif al-Yazan, the Thousand and one Nights, and
various coUections. of stories and novels, such as the Faraj
ba'da 'l-Shidda and the compilation of Bi^AI, well known
by the extracts which Kosegarten has given in his Chres-
tomathy ; — all these show clearly that the Arabs were not
devoid of imagination, at least if, as we believe, these tales
and romances were not pure and simple imitations from
the Persian. It must be acknowledged, however, that these
few productions do not, any more than the Makdmdt of
Hamadhdnl and of Hariri, constitute a very important
literature. The drama, the epic, the romance of character,
were absolutely unknown to the Arabs. Poetry, on the
other hand, an endowment of the ancient Arabs, continued
to live and flourish as long as the Eastern Caliphate lasted.
We may count poets by the hundred, eminent in every
department of that art : in descriptive, erotic, martial, and
philosophic poetry; in odes, in satires, etc. The great
collection entitled Kitdb al-Aghdni,'' compiled by Isftiinl,
contains a choice of the finest poems, accompanied by very
instructive notices of the poets, and of the circumstances
under which they composed such and such pieces. Besides
this, many DlwAns, or complete editions of the works of
poets, have come down to us. They bear the celebrated
names of Nibigha, of 'Antara, of T^rafa, of Zohair, of
'Allfama, of Amraallfais, of Shanfara, of Labid, in the pre-
Islamic period (see Mo'at.t.akat); of Jarir, Akhtal, and
Farazdak,' in the Omayyad period ; and of Abii Nowis,^
Abii 'l-'Atdhiya, Moslim,' Motauabb:* {q.v.), and Abi "1-
■A14,' in the period of the 'AbbAsids. And this list con-
tains only the most illustrious names.
• The first part of wliich has just been published by H. Derenbourg
(Paris, 1882). ' Published by Koshaid Dshdab.
' Tnmsluted by Freytag (Bonn, 1838-43), with the Arabic text of
the proverbs. * See Freytag, Arabische VeTsk^nst.
» Published at Bilik, A.H. 1285 (20 vols ) See also Kosegarten,'
Ali Ispahnnauia tiber canlUmarum, torn. i. Greifswald, 1840.
• See Caussia de Perceval in the Journal asiatijue, 2d scr., vol*,
xiii. liy.
' See Ahlwardt, Die WeingediclUe da Abu iVuuw* (OreiDiwal^
1861 ), and, for a Cairo edition, Z. D. it. O., ixi c74.
• Eilited by De Goeje."
• See Rieu, De Abul.Alcr viix el cannin(bu4, and Kremer ii
Z D. M. a., Jisii., MI., i"L
596
M O H A M M E D A N I S IvI
[science.
With the accession of the 'AbbAsids to power, Moslem
culture entered on a path fruitful in Bcieutilic progress.
The second Caliph of that family, Mansiir, was surrounded
by Syrian Christians of great learning, and equally weU
Transla- acquainted with the Greek, Syriac, and Arabic languages,
tions and took advantage of their abilities to have a number of
^'^'^,'''° foreign books translated into Arabic. Thanks to him, the
■writings of Aristotle, Ptolemy, and Euclid spread a taste
for science among the Moslems. The Caliph Ma'mtin
was one of those who most encouraged translations from
the Greek. In this way the Moslems became acquainted
with the most important productions of -the ancient world.
Plato, the works of the Alexandrian school, those of Hip-
pocrates, Dioscoridos, and Galen, were familiar to them.
Through the Persians many Indian writings also became
accessible to them, such as the fables of Bidpai,' and certain
treatises on astronomy and algebra. The study of philo-
sophy in all its branches was at one time in fashion, and,
to appreciate the success with which it was ciiltivated in
Islam', we need only recall the great names of Al-Kindl,
Al-FdrAbf, Ibn SlnA (Avicenna), Ibn B^ji (Avempace), and
Ibn Eoshd (AveAces), whose scientific teaching swayed
the Middle Ages, and led to the revival of learning in the
West.
History In history and geography, the Moslems distinguished
and geo- themselves. The taste for history had been developed
8"P'"'- among them by the necessity of collecting all traditions
relating to the Prophet, and by that of preserving their own
genealogies. The study of geography was a result of their
conquests. One of their most ancient historical productions
was the biography of Mohammed, composed by Mohammed
b. Ish4k under the caliphate of Mansiir. Wiliddf, another
author of the 8th century of our era, compiled a history of
the first Jiloslem conquests. At a later period, Balddhorf
wrote on the same subject his Kitdb Fotuh al-Bolddn.^
General history also soon became a subject of study, and,
vn the 9th century after Christ, Ibn Kotaiba compiled
kis Kitdb al-Mddrif^ a treatise on universal history. In
the 10th century two great historians flourished, Tabarl
and Mas'iidf, by the first of whom we have a very extensive
chronicle,^ and by the second a general history, entitled
Moriij al-Dhakah (see MAs'uDf). After them came a perfect
galaxy of well-known historians and biographers, such as
Eamza of Isfahdn, Ibn al-Tiktak;i, Nowairi, Makrlzi, Abii
'1-Fidd, Abii '1-Faraj, Al-Makln.'lbn al-AthIr, Soyuti, and Ibn
Kljaldiin,' not to speak of many others who compiled local
chronicles and histories, such as those of Mecca, Medina,
Damascus, and Baghdad. As biographers, Kawawf and
Ibn Khallilf.An " are celebrated. The history of physicians
and philosophers, by Ibn Abl Osaibiya, deserves to be
placed in the first rank, side by side with the history of
religions and sects by ShahrastAniJ
The Moslems were not less active in the study of geo-
graphy. In the 9th century, Ya'lciibi wrote his Kitdb
al-Bolddn, or Book of Countries, in which he described
the principal cities of the Moslem empire.^ After Mm,
Ibn Khordidhbeh comjiosed his Kitdb al-Masdlik wal-
' Translated from the Arabic by KnatcbbuU.
' Edited by Da Goejo (LcyJcn, 1SG6).
' Edited by Wiistcufeld (Gottingen, 1850).
* la course of publication at Loydon, edited by Da Goejo, %vitb tliQ
assistance of J. Earth, Th. Noldeko, P. do Jong, E. Prym, II.
Tliorbeckc, S. FrKultcl, I. Guidi, D. H. Slliller, M, Th. Houtsma,
S. < yard, and V. Rosen.
* -llost of these have been published by Gottwaldt, Ahlwardt,
Keiske, Pocock, Erpenius, Tombcrg.
* The former has been edited by Wiistonfeld (Gottingen, 1842-47),
the latter translated into English by Mac Guokiu de Slaue (Lond.
1343-71).
' Published by Curoton (Lond. 1842-46), and translated into
Carman by HaarbrdckiT (Halle, 1850-51).
« Edited by A. W. Th. JuynboU aud Do Goejo aeydcn, 3SG0-61).
Mamdlik, or Book of Roads and Provinces, in which Lis
principal object is to point out the different routes, and
to give an account of the revenues derived from every
province.' His contemporary Kod-Wa soon after published
his treatise on the work ox clerks, in which, after a notice
of. the various government offices, he gives a descriptiou
of the provinces of the empire witih an account of the
post-routes, their stages and distances, and of the revenues
of each province. AJimed b. Ab( Ya'kilb al-Ya'kiibl wrdte
a description of Asia Minor and Ifrll.dya. Several of
the writings of the historian Mas'iidl also afford highly
valuable information on geography. To Yikut we owe a
great geographical dictionary under the title of Mo'jam
al-Bolddn}" Lastly, Istakhrl, Ibn Hauljal, Mokaddasf,
B^riini, Bakrf, Zamakhshari, Edrisf, and Abii 'l-I'idi
have left us important treatises, narratives of travels, and
geographical dictionaries.^' Among the literatureof voyages
and travels we must also mention ihe curious Chain of
Histories associated with the name of the merchant
Solaimdn and the narratives of Ndsui Khosru,!^ of Ibn
Jobanr," and of Ibn Bati)ta (q.v.).
The sciences connected with geography, such as astro-
nomy and cosmography, were also cultivated by the
Moslems. As early as the reign of Mansiir, the Sanscrit
treatise on astronomy entitled Siddhanta had been trans-
lated into Arabic, Under Ma'miin, two observatories wcro
founded, one at BaghdAd, the other at- Damascus, and
two degrees of the terrestrial meridian were measured by
order of that Caliph. Al-Khirizml, librarian to Ma'miin,
composed his Basm al-Ard, or configuration of the earth,
in which the name of every place was accompanied by it.9
latitude and longitude. Astronomical tables were drawn up
by Yahya, Habash, Abd Ma'shar (Abumazar), and Al-BattAnf
(Albategni). Treatises on astronomy were composed by Al-
Fargh.4ni and Al-Kindl. AJ-Battdni, of whom we have
just spoken, was the author of important works on ,tho
obliquity of the eclij^tio and on the precession of the equi-
noxes. We may m»ntion in the last place the curious
writings of Dimashkf and Kazwinf on general cosmography,
embracing several physical sciences.'''
The study of mathematics was carried very far. The
Moslems not only received arithmetic, geometry, trigo-
nometry, and algebra from the Greeks and Hindus, but
themselves gave a further development to those sciences.
The works of Al-KhArizmf served as guides to those
learned men in Europe who first turned their attention to
algebra in the 16th century .-
The sciences of physics and chemistry, on the other
hand, remained in their infancy. In physical science we
can only mention a few works on Optics. As for Music,
its study was limited to the practical, and though we may
name the important treatise of AJ-Fiirdbl on the theory of
Music — a treatise itself drawn entirely from Greek souice.*
— we must acknowledge that Acoustics, properly so called,
are not at all taken into consideration by him. Chemistrj',
considered as an exact science, continued unkno\vn to the
Moslems ; yet they cultivated Alchemy with eagerness, in
their search after the transmutation of metals, and
Alchemy is the mother of Chcmistiy. Medicine, in the
hands of the Arabs, remained such as they had borrowed
it from the Greeks. As their religion forbade dissection,
the Moslems were never able to rise above a rude empiri-
cism. They contented themselves with adding to their
;niphy.
Matbt
niatics.
ri-.yslc*
MieUM,
' Published and translated by Barbier de Meynard.
'» Edited by ■VVUstcnfeld (Leipzig, 1806-70).
" PuUi.shed, and some translated, by De Goejo, Sachan, WUslonfcld,
Do Grare, Jaubcrt, Dozy, Antari and Scliiaparelli, lUinaud, and De
Slane. Tho last voluino of Abi '1-FiJi'a Gcograjihy is now in the press.
1= Published and translated by Schcfer (Paris, 1831).
IS Edited hy W. Wright (Leydcn, 1852).
" Published and translated by Mchrcn, W'ustcnfcld, and Ethi
fCOlOCEItCE.]
I\I 0 H A M M E D A N I S M
597
own prescriptionSi whicli they pretended to have received
from the Prophet, those of the Greek physicians. The
works of Avicenna prove this ; and Ibn al-BaitAr's treatise
on the pharmacoposia ako shovrs how small a part observa-
tion played in Arabian medicine.^ Zoology, botany, and
mineralogy made no greater progress ; but they were at
least among the subjects which attracted the attention of
learned Moslems. The great treatise by Damirl, entitled
Hay at al-Haiwdn, or Life of Animals, is of interest mainly
from the legends it contains ; ^ and the treatise on miner-
alogy by Taifashi interests ns principally by the details it
gives on the origin of precious stones and the art of cutting
them. It yrouJd be unjust to conclude this sketch without
adding that the Moslems possess also a great number of
technical treatises on the art of war, on military engines,
and the Greek fire, on falconry and hunting, and on
certain industries, such as those of glass, pottery, and
metals. They have also written on magic, on the inter-
pretation of dreams, and on sleight of hand. These works
have as yet been very little investigated. We shall no
doubt find in them interesting revelations on the history
of the industrial arts, and on the history of superstitions.
'■-. With an empire so vast as that of the Moslems, we may
easily conceive how extensive their commerce and industry
must have been, Commerce.had at all times been held in
honour by the Arabs. Long before the days of Mohammed,
the Koraish annually sent caravans, laden with all the
products of Yemen, into Syria. Maritime commerce also
was already flourishing in Chaldaja in the 5th century of
our era. The city of Hlra was frequented by ships coming
from the Red Sea, from India, and even from China.
Obolla was the emporium for the merchandise of India.
It was principally thither that teakwood was brought,
which served for the construction of ships and houses.
Thus the Arabs, when they conquered Chald^a, found
maritime commerce in full activity there, and took advan-
tage of it. Under the 'Abbdsids, Basra supplanted Hlra
and OboUa, and became the principal port. The history
of Sindibid (Sinbad the Sailor) shows how active foreign
commerce was under the 'Abbdsids, and with what courage
the Arab sailors confronted danger. Moslem colonies were
established all along the coasts of Persia and India, and
Moslem voyagers did not fear to venture as far as the
China Seas. On the West, the cormncrcial movement
was not less active. Caravans laden with the products of
Spain left Tangier, traversed the whole of Northern Africa,
and reached Syria, Arabia, and Mesopotamia. Others
passed through Asia Minor, Armenia, Persia, Khorisin,
and TurkestAn, as far as the frontiers of China, while the
route of others again was along the eastern coast of Africa,
whence they brought back ivory and bla6k slaves. Thus
the silks of China, and the spices, camphor, steel, and
precious woods of India, were poureu into the empire ,
while the Moslems exported their glass, their dates, their
cotton stuffs, their refined sugar, and their wrought tools,
to those countries. The manufacture of glass was an .'I, ■;.•■■( .
industry of old standing among them. The glass of Syria '"'^
was celebrated, and we know that flint-glass and enamels
were ako made at Baghdid. Dates were cultivated prin-
cipally in the neighbourhood of Basra, and also in Persia
and Khdzistin. Refined sugar also came from the coast
of Persia. As regards steel, the manufacture of armour
and weapons was the speciality of the people of 'L-dlf, of
Bahrain, of "Om.^n, and of Yemen. The Syrians had ths
credit of forging excellent sword-blades. In Syria t;o
were made mirrors of polished steel. The weaving oi
various stuffs formed an important branch of industry.
The striped stuffs of Yemen, and the tissues of Baghdad,
Herit, Tawwaj, and FasA, enjoyed a high repute. Damas-
cus was renowned for the silk fabrics which have taken
their name from that city. The silks of Yemen, of Egypt,
and of Cufa, had also a high reputation. Timis produced
gauze, and muslin figured with gold. Egypt manufactured
brocade, Armenia supplied satin. The carpet manufacture
imder the Caliphs had already reached the excellence
which it has maintained to our own days. At that time
the carpets most valued came from FArsistan and Tabaric-
tAn. Jewellery and trinkets found numerous outlets, as
may be supposed. This traffic was principally carried on
in the East by the Jews.
We know that the religion of the Prophet forbade any Art
representation of the human figure. This prohibition does
not appear to have been long observed, for we find that
the walls of palaces and of the houses of the rich were
covered with paintings. There was a school of painting
at Basra, and a historian gives us the names of two painters
of high celebrity in their art — Ibn 'Aziz and Kosair.
The manufacture of paper was carried on very extensively,'
a fact which is easily explained when we think of the liter-
ary activity of the Moslems. The Arabs originally used
parchment. For this, after the conquest of Egypt, they
substituted papyrus, which was itself supplanted by paper,
when the Arabs had opened communications with China.
Paper mills were established in several of the provinces,
and at Baghddd itself. Simultaneously with the appear-
ance of this precious substance, the art of binding became
one of the most flourishing industries, as did also the trades
of the shoemaker, the saddler, and the dyer, etc. etc.
Retail commerce, lastly, undertook the distribution of the
products of agriculture and industry. In almost all the
cities of the empire markets were held, where the fruiterer
and grocer {Bakkdl), the butcher (Jazsdr), the armourer
{Saikal), the bookseller (Warrdk), and the druggist and
perfumer ('Attdr), offered their wares for sale.^ (st. g.)
PART III.— THE KORAN.
The Koran (Ko'rAn) is the foundation of Islam. It is the
sacred book of more than a hundred millions of men, some
of them nations of immemorial civilization, by all w.hom it is
regarded as the immediate word of God. And since the
use of the Koran in public worship, in schools and other-
wise, is much more extensive than, for example, the reading
of the Bible in most Christian countries, it has been truly
described as the most widely-read book in existence. This
circumstance alone is sufficient to give it an urgent claim
on our attention, whether it suit our taste and fall in with
our religious and philosophical views or not. Besides, it
is the work of Mohammed, and as such is fitted to afford
The treatise has been translated into French by Dr. Leclerc.
Printed at Bdldk, A.H. 1292.
a clue to the spiritual development of that most successful
of all prophets and religious personalities. It must be
owned that the first perusal leaves on a European an im-
pression of chaotic confusion, — not that the book is so very
extensive, for it is not quite so large as the New Testament.
This impression can in some degree be modified only by the
application of a critical analysis with the assistance of
Arabian tradition.
To the faith of the Moslems, as has been said, the Koran
is the word of God, and such also is the claim which the
book itself advances. For except in sur. i. — which is
' For further information on Moslem civilization, see Kremei'a
important work, CuUurgeschichU (Us OriiiUi unter den CAaltfen,
Vienna, 1875-77.
598
MOHAMMEDANISM
[ko&as.
;a j)rayer for men^and some few passages wnere Moham-
med (vi. 104, Hi; xxv'n. 93; xlii. 8), or the angels
(xlx. 65 ; xxxvii. 164 sqq.), speak in the first person without
the intervention of the usual imperative "say" (sing, or
pi.), the speaker throughout is God, either in the first
person singular, or more commonly the plural of majesty
" we." The same mode of address is familiar to us from
the prophets of the Old Testament ; the human personality
disappears, in the moment of inspiration, behind the God
by whom it is filled. But all the greatest of . the Hebrew
prophets fall back speedily upon the unassuming human
"I"; while in the Koran the divine " I " is the stereotyped
.v.on«m- form of address. Mohammed, however, really felt him-
ii)ed's self to be the instrument of God ; this consciousness was
view of jjQ doubt -brighter at his first appearance than it afterwards
lion. ' b*c^™6, but it never entirely forsook him. We might
therefore readily pardon him for giving out, not only the
results of imaginative and emotional excitement, but ako
many expositions or decrees which were the outcome of
cool calculation, as the word of God, if he had only
attained the pure moral altitude which in an Isaiah or a
Jeremiah fills us with admiration after the lapse of ages.
The rationale of revelation is explained in the Koran itself
'as follo^vs : — In heaven is the original text (" the mother
of the book," xliii. 3 ; "a concealed book," Iv. 77 ; "a well-
guarded tablet," Ixxxv. 22). By a process of "sending
down " (laiizil), one piece after another was communicated
to the Prophet. The mediator was an angel, who is called
sometimss the "Spirit" (xxvi. 193), sometimes the "holy
Spirit" (xvi. 104), and at a later time "Gabriel" (ii. 9l).
This angel dictates the revelation to the Prophet, who
repeats it after him, and afterwards proclaims it to the
world (bcxxvii. 6, etc.). It is plain that we have here a some-
what crude attempt -of the Prophet to represent to himself
the more or less unconscious process by which his ideas
arose and gradually took shape in his. mind. It is no
wonder if in such confused imagery the details are not
always self-consistent. When, for example, this heaveidy
archetype is said to be in the hands of an exalted " scribe "
(Ixxx. 13 sqq.), this seems a transition to a quite different
BPt of ideas, namely, the books of fate, or the record of all
human actions — conceptions which are actually found in
the Koran. It is to be observed, at all events, that
Mohammed's transcendental idea of God, as a Being exalted
altogether above the world, excludes the thought of direct
intercourse between the Prophet and God.
Compon- It is an explicit statement of the Koran that the sacred
tut puis book was revealed ("sent down") by God, not all at once,
Ko«i. ^"^ P^^'=®™'5al and gradually (xxv. 34). This is evident
from the actual composition of the book, and is confirmed
by Moslem tradition. That is to say, Mohammed issued
his revelations in fly-leaves of greater or less extent. A
single piece of this kind was called either, Uke the entire
collection, ko'rdn, i.e. "recitation" or "readinf;" or
Idtdb, "writing;" or stira, which is the late-Hebrew
eUdra, and means literally "series." The last became, in
the lifetime of Mohammed, the regular designation of the
individual sections as distinguished from the whole col-
lection ; and accordingly it is the name given to the sepa-
rate chapters of the existing Koran. These chapters are
of very unequal length. Since many of the shorter ones
are undoubtedly complete in themselves, it is natural to
assume that the longer, which are sometimes very compre-
hensive, have arisen from the amalgamation of various
originally distinct revelations. This supposition is favoured
,by the numerous traditions which give us the circumstances
nnder v.-hich this or that short piece, now incorporated in
a larger section, was revealed ; and also by the fact that
the connection of thought in the present siiras often
s\iras have to be severed out as originally independent ;
even in the short ones parts are often found which cannot
have been there at first. At the same time we must
beware of carrying this sifting operation too far, — as
Noldeke now believes himself to have done in his eailier
works, and as Sprenger also sometimes seems to do.
That some silras were of considerable length from the
first is seen, for example, from xii., which contains
a short introduction, then the history of Joseph, and
then a few concluding observations, and is therefore per-
fectly homogeneous. In like manner, xx., which is mainly
occupied with the history of Moses, forms a complete
whole. The same is true of xviii., which at first sight
seems to fall into several pieces ; the history of the seven
sleepers, the grotesque narrative about Moses, and that
about Alexander " the Horned," are all connected together,
and the same rhyme runs through the whole etlra. Even
in the separate narrations we may observe how readily the
Koran passes from one subject to another, how little care
is taken to express all the transitions of thought, and hov/
frequently clauses are omitted, which are almost indispens-
able. We are not at liberty, therefore, in every case where
the connection in the Koran is obscure, to say that it is
really broken, and set it down as the clumsy patchwork of
a later hand. Even in the old Arabic poetry such abrupt
transitions are of very frequent occurrence. It is not
uncommon for the Koran, after a new subject has been
entered on, to return gradually or suddenly to the former
theme, — a proof that there at least separation is not to be
thought of. In short, however imperfectly the Koran may
have been redacted, in the majority of cases the prei-ciit
suras are identical with the originals.
How these revelations actually arose in Mohammed's
mind is a question wliich it is almost as idle to discU'T as
it would be to analyse the workings of the mind of a poet.
In his early career, sometimes perhaps in its later stages
also, many revelations must have burst from him in uncon-
trollable excitement, so that he could not possibly regard
them otherwise than as divine inspirations. We must
bear in mind that he was no cold systematic thinker, but
an Oriental visionary, brought up in crass superstition,
and mthout intellectual discipline ; a man whose ner-i ous
temperament had been powerfully worked on by ascetic
austerities, and who was all the more irritated by the
opposition he encountered, because he had little of the
heroic in his nature. Filled with his religious ideas and
visions, he might weU fancy he heard the angel bidding
him recite what was said to him. There may have been
many a revelation of this kind which 'no one ever heard
but himself, as he repeated it to himself in the silence of
the night (Ixxiii. 4). Indeed the Koran itself admits
that he forgot some revelations (Ixxxvii. 7). But by far tho
greatest part of the book is undoubtedly the result of deli-
beration, touched more or less with emotion, and animated
by a certain rhetorical rather than poetical glow. Many
passages are based upon purely intellectual reflection. It ia
said that Jlohammed occasionally uttered such a passage im-
mediately after one of those epileptic fits which not only his
followers, but (for a time at least) he himself also, regarded
as tokens of intercourse with the higher powers. If that
is the case, it is impossible to say whether the trick was
in the utterance of tho revelation or in the fit itself.
How the various pieces of the Koran took literary forr; r'
is imcertain. Mohammed himself, so far as wo can dis- K
cover, never wrote down anything. The question whethei-^"
h(j could read and write has been much debated amcn;^
ifoslcms, unfortunately more with dogmatic argumcLll
and spiu-ious traditions than authentic proofs. At present.
»ri,« . i A T '" r I"-^^^"'^"'-^^ »"<=" socms one is inclined to say that he was not altogether il-noran
to be interrupted, ^d m reaLtj many pieces of the long I of these arts, but that from want of pracCho fouud k
Abro.
gated
Headi
K0KAN.1
convenient to employ 8ome one else whenever he had any-
thing to write. After the flight to Medina (a.d. 622) we
are told that short pieces — cliiefly legal decisions — were
taken down immediately after they were revealed, by an
adherent whom he summoned for the purpose; so that
■othing stood in the way of their publication. Hence it
is probable that in Mecca, where the art of writing was
commoner than in Medina, he had already begun to have
his oracles committed to writing. That even long portions
of the Koran existed in written form from an early date
■lay be pretty safely inferred from various indications ;
especially from the fact that in Mecca the Prophet had
caused insertions to be made, and pieces to be erased in
his previous revelations. For we cannot suppose that he
knew the longer s\iras by heart so perfectly that he was
able after a time to lay his finger upon any particular
passage. In some instances, indeed, he may have relied
too much on his memory. For example, he seems to have
occasionally dictated the same silra to different persons in
slightly different terms. In such cases, no doubt, he may
Jiave partly intended to introduce improvements ; and so
long as the difference was merely in expression, without
affecting the sense, it could occasion no perplexity to his
followers. None of them had literary pedantry enough
to question the consistency of the divine revelation on
that ground. In particular instances, however, the differ-
once of reading was too important to be overlooked.
Thus the Koran itself confesses that the unbelievers cast
it up as a reproach to the Prophet that God sometimes
.substituted one verse for another (xvi. 103). On one
occasion, when a dispute arose between two of his own
followers as to the true reading of a passage which both
Lad received from the Prophet himself, Mohanuned is said
to have explained that the Koran was revealed in seven
forms. In this apparently genuine dictum seven stands, of
course, as in many other cases, for an indefinite but limited
number. But one may imagine what a world of trouble
it has cost the Moslem theologians to explain the saying
in accordance with their dogmatic beliefs. A great num-
ber of explanations are curieut, some of which claim the
authority of the Prophet himself; as, indeed, fictitious
utterances of Mohammed play tliroughout a conspicuous
part in the exegesis of the Koran. One very favourite,
but utterly untenable interpretation is that the " seven
forms " are seven different Arabic dialects.
\Vhen such discrepancies came to the cognisance of
Mohammed it was doubtless his desire that only one of
'•* the conflicting texts should be considered authentic; only
he never gave himself much trouble to have his wish
carried into effect. Although in theory he was an up-
holder of verbal inspiration, he did no|t push the doctrine
to its extreme consequences ; his practical good sense did
not take these things so strictly as the theologians of
later centuries. Sometimes, however, he did suppress
whole sections or verses, enjoining his followers to efface
or forget them, and declaring them to be "abrogated."
A very remarkable case is that of the two verses in liii.,
when he had recognised three heathen goddesses as
exalted beings, possessing influence with God. {Supra,
p. 549.)
So mucli for abrogated readings ; the case is somewhat
different when we come to the abrogation of laws and
directions to the Moslems, which often occurs in the
Koran. There is nothing in this at variance with
Mohammed's idea of God. God is to him an absplute
despot, who declares a thing right or \vrong from no
inherent necessity but by his arbitrary fiat. This God
Taries his commands at pleasure, prescribes one law for
the Christians, another for the Jews, and a third for the
Moslems ; nay, he even changes his instructions to the
MOHAMMEDANISM
599
Moslems when it pleases him. Thfis, for example, the
Koran contains verj- different directions, suited to varying
circumstances, as to the treatment which idolaters are to
receive at the hands of believers. . But Mohammed showed
no anxiety to have these superseded enactments destroyed.
Believers could be in no uncertainty as to which of two con-
tradictory passages remained in force ; and they might still
find edification in that which had become obsolete. That
later generations might not so easily distinguish ■'the
" abrogated " from the " abrogating " did - not occur tu
Mohammed, whose vision, naturally enough, seldom ex-
tended to the future of his religious community. , Current
events were invariably kept in view in the revelations.
In Medina it called forth the admiration of the Faithful
to- observe how often God gave them the answer to a
■question whose settlement was urgently required at the
moment. The same naivete appears in a remark of the
Caliph 'Othmin about a doubtful case : 'If the Apostle
of Gfod were stUl alive, methinks there had been a Koran
passage revealed on this point." Not unfrequently the
divine word was found to coincide with the advice which
Mohammed had received from his most intimate disciples.
" Omar was many a time of a certain opinion," says one
tradition, "and the Koran was then revealed accordingly." ,
The contents of the different parts of the Koran areConten*
extremely varied. Many passages consist of theological orof tJ";
moral reflections. We are reminded of the greatness, the^'^""^
goodness, the righteousness of God as manifested in Nature,
in history, and in revelation through the prophets, especially
through Mohammed. God is magnified as the One, the
All-powerful Idolatry and all deification of created beings,
such as the worship of Christ as the Son of God, are un-
sparingly condemned. The joys of heaven and the pains
of hell are depicted in vivid sensuous imagery, as is also
the terror of the whole creation at the advent of the last
day and the judgment of the world. Believers receive
general moral instruction, as well as directions for special
circumstances. The lukewarm are rebuked, the enemies
threatened with terrible punishment, both temporal and
eternal. To the sceptical the truth of Islam is held forth ;
and a certain, not very cogent, method of demonstration
predominates. In many passages the sacred book falls into
a diffuse preaching style, others seem more like proclama-
tions or general orders. A great number contain ceremonial
or civil laws, or even special commands to individuals down
to such matters as the regulation of Mohammed's harem.'
In not a few, definite questions are answered which had
actually been propounded to the Prophet by believers or
infidels. Mohammed himself, too, repeatedly receives direct
injunctions, and does not escape an occasional rebuke. Ona
siira (i.) is a prayer, two (cxiii., cxiv.) are magical formulas.*
Mafiy suras treat of a single topic, others embrace several.!^
From the mass of material comprised in the Koran — and Kari»»
the account we have given is far from exhaustive — we''i''ea.
should select the histories of the ancient prophets i\.a^\
saints as possessing a peculiar interest. The purpose oi
Mohammed is to show from these histories how God in
former times had rewarded the righteous, and punished
their enemies. For the most part the old prophets only
serve to introduce a little variety in point of form, for they
are almost in every case facsimiles of Mohammed himself.
They preach exactly like him, they have to bring the very
same charges against their opponents, who on their part
behave exactly as the unbelieving inhabitants of Mecca.
The Koran even goes so far as to make Noah contend
against the worship of certain false gods, mentioned by
name, who were worshipped by the Arabs of Mohammed's
time. . In an address which is put in the mouth of Abra
ham (xxvi. 75 sqq.) the reader quite forgets that it i.;
Abraham, 'and not Mohammed (or God hunself)'who ia
600
3^, O H A M M E D A N I S M.
[kohan.
s
Eehtios
to the
Old U!;.\
Now T< '■■
twueni—
speaking. Other narratives are intended rather for amuse-
ment, although they are always well seasoned with edifying
phrases. It is no wonder that the godless Koraishites
thought these stories of the Koran not nearly so entertain-
ing as those of Rostam and Ispandiar related by Nadr the
son of Hiirith, who had learned on the Euphrates the
heroic mythology of the Persians. But the Prophet was
so exasperated by this rivaliy that when Nadr fell into his
power after the battle of Badr, he caused him to be executed ;
although in all other cases he readily pardoned his fellow-
countrj'men.
These histories are chiefly about Scriptm-e characters,
especially those of the Old Testament. But the deviations
from the Biblical narratives are very marked. Many of
the alterations are found in the legendary anecdotes of the
Jewish Haggada and the New Testament Apocrypha ; but
many moVe are due to misconceptions such as only a listener
(not the reader of a book) coiild fall into. The most igno-
rant Jew could never have mistaken Haman (the minister
of Ahasuerus) . for the minister of Pharaoh, or identified
Miriam the sister of Moses with Mary ( = Miriam) the
mother of Christ. In addition to such misconceptions
there are sundry capricious alterations, some of them very
'grotesque, due to Mohammed himself. For instance, in
his ignorance of everything out of Arabia, he .makes the
fertility of Egypt — where rain is almost never seen and never
missed — depend on rain instead of the inundations of the
Nile (xii. 49). It was through the Jews also that he
borrowed his accotint of Ale.xander " the Horned " ; an
epithet which is to be explained, after old Hettinger, from
the great multitude of coins where Alexander is represented
with the ram's-horn of Ammon. Besides Jewish and
Christian histories there are a few about oldi Ai-abian
prophets. In these he seems to have handled his materials
even more freely than in the others.
The opinion has already been expressed that Mohammed
idid not make use of written sources. Coincidences and
[divergences alike can always be accounted for by oral com-
munications from Jews who knew a little and Christians
(who knew next to nothing. Even in the rare passages
Avhere we can trace direct resemblances to the text of the
Old Testament (comp. xxi. 105 with Ps. xxxvii. 29 ; i. 5 with
Ps. xxvii. 11) or the New (comp. vii. 48 'n'ith Luke xvi. 24 ;
xlvi. 19 with Luke xvi. 25), there is notliing more than
might readily have been picked up in conversation with
any Jew or Christian. In Medina, where he had the
opportunity of becoming acquainted with Jews of some
culture, he learned some things out of the Mishna, e.tj.
V. 35 corresponds almost word for word v.ith Mishna Sank.
iV. 5; compare also ii. 183 with Mishna Ber. i. 2. That
these are only cases of oral communication wiU be admitted
by any on?v with ttt slightest knowledge of the circum-
stances. Other^vi3e !\ e might even conclude that Moham-
med had studied the Talmud ; e.g. the regulation as to
ablution by rubbing with sand, where water cannot be
obtained (iv. 4C), corresponds to a talmudic ordinance
{^Ber. 15 a). Of Christianity he can have been able to learn
very little even in Medina ; as may be seen from the absiu'd
travesty of the institution of the Eucharist in v. 112 sqq.
For the rest, it is highly improbable that before the Koran
any real literary production — anything that could be
strictly called a book — existed in the Arabic language.
In point of style and artistic effect, the different parts
of the Koran are of very unequal value. An unprejudiced
and critical reader will certainly find very few passages
where his a'sthetic susceptibilities are thoroughly satisfied.
But he will often bo struck, especially in the older pieces,
by a wild force of passion, and a vigorous, if not rich,
imagination. Descriptions of heaven and hell, and allu-
sions to God's working in Nature, hot unfrequently show
a certain amount of poetic power. In other places also
the style is sometimes Uvely and impressive ; though it is
rarely indeed that we come across such strains of touching
simplicity as in the middle of xciii. The greater part of the
Koran is decidedly prosaic ; much of it indeed is stiff in style.
Of course, with such a variety of material, we cannot expect
every part to be equally vivacious, or imaginative, or
poetic. A decree about the right of inheritance, or a
point of ritual, must necessarily be expressed in prose, if
it is to be inteUigible. No one complains of the civil lav.s
in Exodus or the sacrificial ritual in Leviticus, becai'se
they want the fire of Isaiah or the tenderness of Deuter-
onomy. But Mohammed's mistake consists in persistent
End slavish adherence to the semi-poetic form which he
had at first adopted in accordance with his own taste and
that of his hearers. For instance, he employs rhyme i i
deahng with the most prosaic subjects, and thus produce*
the disagreeable effect of incongruity between style and
matter. It has to be considered, however, that many of
those sermonizing pieces which are so tedious to us, especi-
ally when we read two or three in succession (perhaps in
a very inadequate translation), ■ must have had a quit o
different effect when recited under the burning sky anl
on the barren soil of Mecca. There, thoughts about
God's gi'eatness and man's duty, which are familiar to «>
from childhood, were all new to the hearers — it is hearei ;
we have to think of in the first instance, not readers — to
whom, at the same time, every allusion had a meanin.;.'
which often escapes oiu- notice. When Mohammed spoko
of the goodness of the Lord in creating the clouds, and
bringing them across the cheerless desert, and pouring
them out on the earth to restore its rich vegetation, that
must have been a picture of thrilling interest to the Arabs,
who are accustomed to see from three to five years elapse
before a copious shower comes to clothe the wilderness
once more with luxuriant pastures. It requires an effort
for us, under our clouded skies, to realize in some degree;
the intensity of that impression.
The fact that scraps of poetical phi-aseology are spe- '
cially numerous in the earlier siiras, enables us to undc ■-
stand why the prosaic mercantile community of Mecca ■
regarded their eccentric to'svnsman as a " poet," or even a
"possessed poet." Jlohammed himself had to disclaim
such titles, because he felt himself to be a divinely-inspired
prophet ; but we too, from our standpoint, shall full;.'
acquit him of poetic genius. Like many other predom'-
nantly religious characters, he had no appreciation of poet -J
beauty ; and if we may believe one anecdote related of
him, at a time when every one made verses he affected
ignorance of the most elementary rules of prosody. Hero
the style of the Koran is not poetical but rhetorical ; and,
the powerful effect which some portions produce on us is
gained by rhetorical means. Accordingly the sacred bool:
lias not even the artistic fonn of poetry ; which, among
the Arabs, includes a stringent metre, as well as rliymc.
The Koran is never metrical, and only a few exceptionally
eloquent.portions fall into a sort of spontaneous rhythm. 0'\
theother hand, the rhyme is regularly maintained ; although,
especially in the later pieces, after a very slovenly fashion.
Hhymed prose was a favourite form of composition among
tlie Arabs of that day, and Jlohammed adopted it ; but
if it imparts a certain sprightliness to some passages, it
proves on the whole a burdensome yoke. The Moslems
themselves have observed that the tyranny of the rhyme
often makes itself apparent in derangement of the ordi r
of words,, and in the choice of verbal forms which wouli
not otheiWise have been employed ; e.g. an imperfect instead
of a perfect. In one place, to save the rhyme, ho cal'.<
Mount Sinai S;n',:i (xcv. 2) instead of SlnCt (xxiii. 20^ ;
in another Elijah is called Ilt/dsm (xxxvii. 130) instead oi
\1 lone
KOEAN.J
MOHAMMEDANISM
601
jf the
Hyds (vL 85; xxrrii. 123). The substance even is nicxii-
fiol to suit exigencies of rhyme. Thus the Proj-iiet -would
scarcely have fixed on the unusual number of eight angels
round the throne of God (Ixix. 17) if the word thamdniyah,
"eight," had not happened to fall in so well with the
rhyme. And when Iv. speaks of two heavenly gardens,
each with txao fountains and ttoo kinds of fruit, and again
of tun similar gardens, all this is simply because the dual
termination (<(») corresponds to the syllable that controls
the rhyme in that whole siira. In the later pieces,
Mohammed often inserts edifying remarks, entirely out of
keeping with the context, merely to complete his rh3rme.
In Arabic it is such an easy thing to accumulate masses
of words with the same termination, that the gross negli-
gence of the rhyme in the Koran is doubly remarkable.
One may say that this is another mark of the Prophet's
want of mental training, and incapacity for introspective
criticism.
On the whole, while many parts of the Koran tm-
doubtedly have considerable rhetorical power, even over
an unbelieving reader, the book, aesthetically considered,
is by no means a first-rate performance. To begin with
what we are most competent to criticize, let us look at
some of the more extended narratives. It has already
been noticed how vehement and abrupt they are where
they ought to be characterized by epic repose. Indispens-
able links, both in expression and in the sequence of
events, are often omitted, so that to understand these
histories is sometimes far easier for us than for those who
heard them first, because we know most of them from
better sources. Along with this, there is a great deal of
superfluous verbiage ; and nowhere do we find a steady
advance in the narration. Contrast in these respects the
history of Joseph (xii.) and its glaring improprieties, with
the admirably-conceived and admirably-executed story in
Genesis. Similar faults are found in the non-narrative
portions of the Koran. The connexion of ideas is
extremely loose, and even the syntax betrays great awk-
■wardness. Anacolutha are of frequent occurrence, and
cannot be explained as conscious literary devices. Many
sentences begin with a " when " or " on the day when "
wiiich seems to hover in the air, so that the commentators
are driven to supply a " think of this " or some such
ellipsis. Again, there is no great literary skill evinced in
the frequent and needless harping on the same words and
phrases ; in xviii., for example, " till that ' {hatid idhd)
occurs no fewer than eight times. Mohammed, in short,
is not in any sense a master of style. This opinion will
be endorsed by any European who reads through the
book with an impartial spirit and some knowledge of the
Unguage, without taking into accoimt the tiresome effect
sf its endless iterations. But in the ears of every pious
Moslem such a judgment wiU sound almost as shocking as
lownright atheism or polj-theism. Among the Moslems,
the Koran has always been looked on os the most perfect
model of style and language. This feature of it is in
their dogmatic the greatest of all miracles, the incontest-
able proof of its divine origin. Such a view on the part
of men who knew Arabic infinitely better than the most
accomplished European Arabist will ever do, may well
startle us. In fact, the Koran boldly challenged its
opponents to produce ten suras, or even a single one, like
those of the sacred, book, and they never did so. That,
to be sure, on calm reflexion, is not so very surprising.
Revelations of the kind which Mohammed uttered, no
unbeliever could produce without making himself a laugh-
ing-stock. However little real originality there is in
Mohammed's doctrines, as against his own countrymen
he was thoroughly original, even in the form of his oracles.
To compoce such revelatioas at will was beyond the rjower
IG— 22*
of the most expert literary artist; it would have required
either a prophet, or a shameless impostor. And if such a
character appeared after Mohammed, still he could never
be anything but an imitator, like the false prophets who
arose about the time of his death and aftenvards. That
the adversaries should produce any sample whatsoever of
poetry or rhetoric equal to the Koran is not at all what
the Prophet demands. In that case he would have been
put to shame, even in the eyes of many of his own
followers, by the first poem that came to hand. Never-
theless, it is on a false interpretation of this challenge that
the dogma of the incomparable excellence of the style and
diction of the Koran is based. The rest has been accom-
plished by dogmatic prejudice, which is quite capable of
working other miracles besides turning a defective literary
production into an imrivalled masterpiece in the eyes of
believers. This view once accepted, the next step was to
find everywhere evidence of the perfection of the style and
language. And if here and there, as one can scarcely
doubt, there was among the old Moslems a lover of poetry
who had his difficulties about this dogma, he had C>
beware of uttering an opinion which might have cost him
his head. We know of at least one rationalistic theologiaa
who defined the dogma in such a way that we can see.
he did not beheve it (Shahrastinl, p. 39). The truth is,
it would have been a miracle indeed if the style of the
Koran had been perfect. For although there was at that
time a recognized poetical style, already degenerating to
mannerism, a prose style did not exist. All beginnings
are difficult ; and it can never be esteemed a serious
charge against Mohammed that his book, the first prose
work of a high order in the language, testifies to the awk-
wardness of the beginner. And further, we must always
remember that entertainment and sesthetic effect were at
most subsidiary objects. The great aim was persuasion
and conversion ; and, say what we will, that aim has been
realized on the most imposing scale.
Mohammed repeatedly calls attention to the fact that the Fcreiga
Koran is not written, like other sacred books, in a strange wordi.
language, but in Arabic, and therefore is intelligible to
all. At that time, along ■nith foreign ideas, many foreign
words had crept into the language ; especially Aj-amaic
terms for religious conceptions of Jewish or Christian
origin. Some of these had already passed into general
use, while others were confined to a more limited circle.
Mohammed, who could not fuUy express his new ideas in
the common language of his countrjrmen, but had frequently
to find out new terms for himself, made free use of sucli
Jewish and Christian words, as was done, though perhaps to
a smaller extent, by certain thinkers and poets of that age
who had more or less risen above the level of heathenism.
In Mohammed's case this is the less wonderful, because he
was indebted to the instruction of Jews and Christians
whose Arabic — as the Koran pretty clearly intimates with
regard to one of them — was very defective. Nor is it
very surprising to find that his use of these words is some-
times as much at fault as his comprehension of the
histories which he learned from the same people — that he
applies Aramaic expressions as incorrectly as many unedu-
cated persons now employ words derived from the French.
Thus, foi-yan means really " redemption," but Mohammed
(misled by the Arabic meaning of the root j_^ "sever,"
"decide") uses it for "revelation." Milla is properly
" Word," but in the Koran " religion." UliyiU (Ixxxiii.
IS, 19) is apparently the Hebrew name of God, E/yon,
" the Most High " ; Mohammed uses it of a heavenly book
(see S. Fraenkel, J)e vocahulis in antiguis Arabum carmin-
ibus et in Corano peregrinis, Leyden, ISSO, p. 23). So
again the word mcUhdni is, as Geiger has conjectm-ed, tha
602
M O H A M M E D A iS 1 S M'
I KORAN."
re'nilar plural of tlie Aramaic TimthnUhd, which is the
same as the Hebrew Miskna, and denotes, in Jewish usage,
a leal decision of some of the ancient Rabbins. But in
the Koran "the seven Math&ni" (xv. 87) are probably
the seven verses of siira i., so that Mohammed appeai-s to
have understood it in the sense of "saying," or "sen
tence" (comp. xxxix. 24). Words of Christian origin are
Jess frequent in the Koran. It is an interesting fact
tliat tf thesf; a few have come over from the Abyssinian ;
such as haivdrii/un, " apostles," mdida, " table," and two
or three others ; these all make their first appearance in
siiras of the Medina period. The word shaitdn, "Satan,"
w uich was likewise borrowed, at least in the first instance,
from the Abyssinian, had probably been already intro-
duced into the language. Sprenger has rightly observed
that Mohammed makes a certain parade of these foreign
terms, as of other peculiarly constructed expressions ; in
tliis he followed a favourite practice of contemporary poets.
It is the tendency of the imperfectly educated to delight
in out-of-the-way expressions, and on such minds they
readily produce a remarkably solemn and mysterious
impression. This was exactly the kind of effect that
Jfohammed desired, and to secure it he seems even to
have invented a few odd vocables, as ghislin (Ixix. 36),
tijjin (Lxx.xiii. 7, 8), tasnim (l.xxxiii. 27), and salsahil (Ixxvi.
18). But, of course, the necessity of enabling his hearers
to understand ideas which they must have found suffi-
ciently novel in themselves, imposed tolerably naiTOw
limits on such eccentricities.
Dale of The constituents of our present Koran belong partly to
tlieseve- the Mecca period (before 622 A.D.), partly to the period
rri parts, ^.ommencing with the flight to Medina (from the autumn
of 622 to 8th June 632). Mohammed's position in Medina
was entirely different from that which he had occupied in
his native to^vn. In the former he was from the first the
loader of a powerful party, and gradually became the
autocratic ruler of Arabia ; in the latter he was only the
despised preacher of a small congregation. This difference,
ns was to be expected, appears in the Koran. The Medina
j'ieces, whether entire siiras or isolated passages interpo-
lated in Meccan siiras, are accordingly pretty broadly dis-
tinct, as to their contents, from those issued in Mecca.
In the great majority of cases there can be no doubt what-
ever whether a piece first saw the light in Mecca or in
Jledina ; and for the most part the internal evidence is
borne out by Moslem tradition. And since the revelations
given in Medina frequently take notice of events about
which we have pretty accurate information, and whose
dates are at least approximately kn'.wn. We are often in a
position to fix their date with at any rate considerable
certainty ; here again tradition rendera valuable assistance.
Even with regard to the Medina passages, however, a great
deal remains uncertain, partly because the allusions to
historical events and circumstances are generally rather
obscure, partly because traditions about the occasion of
the revelation of the various pieces are often fluctuating,
and often rest on misunderstanding or arbitrary conjecture.
JiUt at all events it is far easier to arrange in some sort of
chronological order the Medina siiras than those composed
in Mecia. There is, indeed, one tradition which professes
to furnish a chronological list of all the siiras. But not to
mention that it occurs in several divergent forms, and that
it takes no account of the fact that our present siiras are
]'artly composed of pieces of different dates, it contains so
many Bus|)iciou3 or undoubtedly false statements, that it
ii impossible to attach any great importance to it. Besides,
it is a ptiori unlikely that a contemporary of Mohammed
should have drawn up such a list ; and if any one had
made the attemjit, ho would have found it almost impos-
sible to obtain reliable infurmation as to tlio order of the
earlier Meccan siiras. We have in this list no genuine
tradition, but rather the lucubrations of .an undoubtedly
conscientious Moslem critic, who may have lived about a
century after the Flight.
Among the revelations put forth in Mecca there is 6 The
considerable number of ^for the most part) short siiras, MeeoaL
which strike every attentive reader as being the oldest.: ^™^'
They are in an altogether different strain from many others,'
and in their whole composition they show least resemblance
to the Medina pieces. It is no doubt conceivable — as
Sprenger supposes — that Mohammed might have returned
at uitervals to his earlier manner ; but since this group
possesses a remarkable similarity of style, and since the
gradual formation of a different style is on the whole an
unmistakable fact, the assumption has little probability ;
and we shall therefore abide by the opinion that these
form a distinct group. At the opposite extreme from
them stands another cluster, showing quite obvious affinities
with the style of the Medina siiras, which must therefore
be assigned to the later part of the Prophet's work in
Mecca. Between these two groups stand a number of
other Meccan siii'as, which in every respect mark the
transition from the first period to the third. It need
hardly be said that the three periods — which .were first
distinguished by Professor Weil — are not separated by
sharp lines of division. With regard to some siiras, it may
be doubtful whether they ought to be reckoned amongst
the middle group, or with one or other of the extremes.
And it is altogether impossible, within these groups, to
establish even a probable chronological arrangement of the
individual revelations. In default of clear allusions to
w'ell-knowu events, or events whose date can be deter-
mined, we might indeed endeavom' to trace the psycholo-
gical development of the Prophet by means of the Koran,
and arrange its parts accordingly. But in such an under-
taking one is always apt to take subjective assumptions
or mere fancies for established data. Good traditions
about the origin of the Meccan revelations are not very
numerous. In fact the whole history of Mohammed
previous to the Flight is so imperfectly related that we
are not even sure in what year he appeared as a prophet.
Probably it was in a.d. 610; it may have been somewhat
earlier, liut scarcely later. If, as one tradition says, xxx.
1 sq. ("The Romans are overcome in the nearest neigh-
bouring land ") refers to the defeat of the Byzantines by
the Persians, not far from Damascus, about the spring of
614, it would follow that the third group, to which this
passage belongs, covers the greater part of the Jleccan
period. And it is not in itself unlikely that the passionate
vehemence which characterizes the first group was of short
duration. Nor is the assumption contradicted by the
tolerably woU-attosted, though far from incontestable state-
ment, that when 'Omar was converted (a.b. 615 or G16),
XX., which belongs to the second gioup, already existed
in writing. But the reference of xxx. 1 sq. to this particu-
lar battle is by no means so certain that positive conclu-
sions can be drawn from it. It is the same with other
allusions in the Meccan siiras to occurrences whose chrono-
logy can be partially ascertained. It is better, therefore, to
rest satisfied with a merely relative determination of the
order of even the three great clusters of Meccan revelations.
In the pieces of the first period the convulsive excite- OUr^t
mcnt of the Prophet often expresses itself with the utmost Meicin
vehemence. Ho is so carried away by his emotion that,*"*^'
he cannot choose his words ; they seem rather to burst
from him. Many of those pieces remind us of the oracles
of the old heathen soothsayers, whose style is known to
us from imitations, although we have perhaps not a single
genuine specimen. Like those other oracles, the siiras of
this period, which are never very long, are composed of
■SOBOJ.J
MOHAMMEDANISM
603
The
fitihs,
'short sentences withTblerabiy pure but rapidly-changing
rhymes. The oaths, too, with which many of them begin,
■were largely used by the soothsayers. Some of these
oaths are very uncouth and hard to understand, some of
them perhaps were not meant to be understood, for indeed
all sorts of strange things are met with in these chapters.
Here and there Mohammed speaks of visions, and appears
even to see angels before him in bodily form. There are
some intensely vivid descriptions of the resurrection and
the last day which must have exercised a demonic power
over men who were quite unfamiliar with such pictures.
Other pieces paint in glowing colours the joys of heaven
and the pains of hell. However, the siiras of. this period
are not all so wild as these ; ^d those which are conceived
in a calmer mood appear to be the oldest. Yet, one must
repeat, it is exceedingly difficult to make out any strict
chronological sequence. For instance, it is by no means
certain whether the beginning of scvi. is really, what a
widely-circulated tradition calls it, the oldest part of the
whole Koran. That tradition goes back to the Prophet's
favourite wife 'Aisha ; but as she was not bom at the
time when the revelation is said to have been made, it
cau only contain at the best what Mohammed told her
years afterwards, from his oivn not very clear recollection,
with or without fictitious additi9ns. And, moreover,
there are other pieces mentioned by others as the oldest.
In any case xcvi. 1 sqq. is certainly very early. Accord-
ing to the traditional view, which appears to be correct,
it treats of a vision in which the Prophet receives an
injunction to recite a revelation conveyed to him by the
angel. It is interesting to observe that here already two
things are brought forward as proofs of the omnipotence
and care of God : one is the creation of man out of a
seminal drop — an idea to which Mohammed often recurs ;
the other is the then recestly introduced art of writing,
which the Prophet instinctively seizes on as a means of
propagating his doctrines. It was only after Mohammed
encountered obstinate resistance that the tone of the reve-
lations became thoroughly passionate. In such cases he
was not slow to utter terrible threats against those who
ridiculed the preaching of the unity of God, of the resur-
rection, and of the judgment. His own uncle Abu Lahab
had rudely repelled him, and in a brief special siira (cxi.)
he and his wife are consigned to hell. The siiras of this
period form almost exclusively the concluding portions of
the present text. One is disposed to assume, however,
that they were at one time more numerous, and that many
of them were lost at an early period.
Since Mohammed's strength lay in his enthusiastic and
fiery imagination rather than in the wealth of ideas and
clearness of abstract thought on which exact reasoning
depends, it follows that the older siira% in which the
former qualities have free scope, must be more attractive
to us than the later. In the silras of the second period
the imaginative glow perceptibly diminishes ; there is still
fire and animation, but the tone becomes gradually more
prosaic. As the feverish restlessness subsides, the periods
are drawn out, and the revelations as a whole become
longer. The truth of the new doctrine is proved by accu-
mulated instances of God's working in nature and in
history ; the objections of opponents, whether advanced
in good faith or in jest, are controverted by argimients ;
but the demonstration is often confused or even weak.
_ The histories of the earlier prophets, which had occasion-
ally been briefly touched on in the first period, are now
related, sometimes at great length. On the whole, the
harm of the style is passing away.
There is one piece of the Koran, belonging to the begin-
ning of this period, if not to the close of the former, which
claims particular notice. This is i., the Lord's Prayer of
the'Moslems, and beyond dispute the gem of the Koran.
The words of this s>lra, which is known as al-fdtiha (" the
opening one ") are as follows : —
(1) In the name of God, tlie compassionate compassioner. (2>
Praise be [literally "is"] to God, the Lord of the worlds, (3) tho
comp,issionate compassioner, (4) the Sovereign of tho day of
judgment. (5) Thee do wo worship and of Thee do wo beg assist-
ance. (6) Direct us in the right way ; (7) in the way of those to
whom 'Thou hast been gracious, on whom there is no wrath, and
who go not astray.
The thoughts are so simple as to need no explanation ;
and yet the prayer is full of meaning. It is true that
tiiere is not a single original idea of Mohammed's in it.
Several words and turns of expression are borrowed diiectly
from the Jews, in particular the designation of God as the
" Coigpassioner," Rahmdn. This is simply the Jewish Rabmla
Rahmdnd, which was a favourite name for God in the
Talmudic period. Mohammed seems for a while to have
entertained the thought of adopting al-Ro.hmdn as a proper
name of God, in place of AUdk, which was already used by
the heathens.^ This purpose he ultimately relinquished,
but it is just in the siiras of the second period that the use
of Rahvidii is specially frequent. It was probably in tho
first siira also that Mohammed first introduced the formula,
" In the name of God," etc. It is to be regretted that this
prayer must lose its effect through too frequent use, for
every Moslem who says his five prayers regularl)' — as the
most of them do — repeats it not less than twenty iimes
a day.
The siiras of the third Meccan period, which form aLatcai
pretty large part of our present Koran, are almost entirely Meccai»
prosaic. Some of the revelations are of considerable""*''
extent, and the single verses also are much longer than
in the older siiras. Only now and then a gleam of poetic
power flashes out. A sermonizing tone predominates.
The siiras are very edifying for one who is already recon-
ciled to their import, but to us at least they do not seen*
very well fitted to carry conviction to the minds of unbe-
lievers. That impression, however, is not correct, for ■ in
reality the demonstrations of these longer Jleccan siiras
appear to have been peculiarly influential for the propaga-
tion of Islam. Mohammed's mission was not to Europeans,
but to a people who, though quick-witted and receptive, were
not accustomed to logical thinking, while they had out-
grown their ancient religion.
When we reach the Medina period it becomes, as hasMedim
been indicated, much easier to understand the revelation^ siii"-
in their historical relations, since our knowledge of the
history of Mohammed in Medina is tolerably complete. ■
In many cases the historical occasion is perfectly clear. .
in others we can at least recognize the general situation,
from which they arose, and thus approximately fix their
time. There still remains, however, a remnant, of which
we can only say that it belongs to Medina.
The style of this period bears a pretty close resemblance
to that of the latest Meccan period. It is for the most
part pure prose, enriched by occasional rhetorical embellish-
ments. Yet even here there are many bright and impres-
sive passages, especially in those sections which may be
regarded as proclamations to the army of the faithful. For
the Moslems, Mohammed has many different messages. At
one time it is a summons to do battle for the faith ; at
another, a series of reflexions on recently experienced success
or misfortune, or a rebuke for their weak faith ; or an ex-
hortation to virtue, and so on. He often addresses himself
to the " doubters," some of whom vacillate between faitl
and imbelief, others make a pretence of faith, while othen
' Since in Arabic also the root (.»j signifies " to have pity." tl«
Arabs must have at once perceived the force of the new name.
604
M O H A M M E D A N i S M
[korax.
scarcely take tlio tiouble even to do that. They are no
consolidatsd l)aity, but to Mohammed they are all equally
vexatious, because, as boon as danger has to be encountered,
or a contribution is levied, they all alike fall away. ' There
are frequent outburst?, ever increasing in bitterness, against
the .lews, who were very numerous in Medina and its
neighbourhood when Mohammed arrived. Ho has much
less to .'■ay against the Christians, with whom he never
came closely in contact ; and as for the idolaters, there was
little occasion in Medina to have many words -n'ith them.
A part of the Medina pieces consists of formal laws belong-
ing to the ceremonial, civil, and criminal codes ; or directions
about certain temporary complications. The most objec-
tionable parts of the whole Koran are those which treat of
Mohammed's relations with women. The laws and regula-
tions were generally very concise revelations, but most of
them have been amalgamated with other pieces of similar
or dissimilar import, and are now found in very long silras.
Such is an imperfect sketch of the composition and the
internal liistory of the Koran, but it is probably sufficient
to show that the book is a very heterogeneous collection.
If only those passages had been preserved which had a
permanent value for the theology, the ethics, or the juris-
prudence of the Jloslems, a few fragments would have been
amply sufficient. Fortunately for knowledge, respect for
the sacredness of the letter has led to the collection of all
the revelations that could possibly be collected, — the " abro-
gating" along with the "abrogated," passages referring to
passing circumstances as well as those of lasting importance.
Every one who takes up the book in the proper religious
frame of mind, like most of the Moslems, reads pieces
directed against long-obsolete absurd customs of Mecca
just as devoutly as the weightiest moral precepts, — perhaps
even more devoutly, because he does not understand them
so well. ._
At. the head of tweuty-niue oi tne suras staud certain mitial
letters, from which no clear sense can be obtained Thus, before
ii. iii. xxxl. xx.^i. we find JJ {Alif Ldm Mlm), before xl.-xlvi.
..j» tna Mlm). Kbldeke at one tiine suggested that these initials
r ■
did not belong to Mohammed's text, but might be the monograms
of iJOSsessoi"s of codices, which, through negligence on the part of
the editors, were incorporated in the final form of the Koran ;
lie now deems it move probable that they are to be traced to the
Prophet himself, as Spren^er, Loth, and others suppose. One can-
not indeed admit the truth of Loth's statement that in the proper
opening words of these suras we may generally find an allusion to
the accompanying initials ; but it can scarcely be accidental that
the first verse of the great majority of them (in iii. it is the second
verse) contains the word ** book," *' revelatioi^" or some equivalent.
They usually begin with: "This is the look," or "Revelation
('down sending') of the book," or something similar. Of suras
which commence in this way only a few (xviii. xxiv. xxv. xxxix. )
want the Initials, while only xxix. and xxx. have the initials ami
begin dilTerently. These few exceptions may easUy have proceeded
from ancient corruptious ; at all events they cannot neutralize the
evidence of the greater number. Mohammed seems to have meant
these letters for a mystic reference to the archetypal text in heaven.
To a man who regarded the art of writing, of which at the best he had
but a slight knowledge, as something supernatural, and who lived
amongst illiterate people, an A B C may well have seemed more sig-
nificant than to us who have been initiated into the mysteiies of this
art from our childhood. The Prophet himself can h.ardly have
attached any particular meaning to these symbols : they served their
purpose if they conveyed an impression of solemnity and enigmatical
obscurity. In fact, the Koran admits that it contains many things
which neither ca.i ^'e, nor were intended to be, imderstood (iii. 6).
To regard these letters as ciphers is a precarious hypothesis, for the
simple reason that crj-ptography is not to be looked for in the very
infancy of Arabic writing. If they are actually ciphers, the multipli-
city of possible explanations at once precludes the hope of a plausible
interpretation. None of the olTorta in this direction, whether by
Moslem scholars or by Europeans, have led to convincing results.
Tliis remark applies even to the ingenious conjectm'e of Sprenger,
that the letters (_,aj!-4^=. {KAf Iii Yt 'Aim. Sid) before six. (which
treats of John and Jesus, and, according to tradition, w.xi sent
to tho Christian king if Ab-jsaiuia) ctan>l for Juna A'marm-M
RfT Juaecorum. Sprenger arrives at this explanation by a very
artificial method ; and besides, Mohammed was not so simple as the
Moslem traditionalists, who imagined that the Abyssinians could
read a piece of the Arabic Koran. It need hardly be said that the
Moslems have from of old applied themselves with great assiduity to
the decipherment of these initials, and have sometimes found the
deepest mysteries in them. Ge.neral]y, however, they are content
with the prudent conclusion, that God alone knows the meaning of
these letters.
AVhen Mohammed died, the separate pieces of the Koran, Tram-
notwithstanding their theoretical sacredness, existed only missior
in scattered copies ; they were consequently in great danger °' "■*
of being partially or entirely destroyed. Many Moslems ^"'"•
knew large portions by heart, but certainly no one knew
the whole ; and a merely oral propagation would have left
the door open to all kinds of deliberate and inadvertent
alterations. Jlohammed himself had never thought of an
authentic collection of his revelations; he was usually
concerned only ivith the object of the moment, and the idea
that the revelations would be destroyed unless he made pro-
vision for their safe preservation, did not enter his mind.
A man destitute of literary culture has some difficulty in
anticipating the fate of intellectual products. But now,
after the death of the Prophet, most of the Arabs revolted
against his successor, and had to be reduced to submission
by force. Especially sanguinary was the contest against
the prophet !Maslama (Mubarrad, Kdmil 443, 5), an imi-
tator of Mohammed, commonly known by the derisive
diminutive Mosailima. At that time (a.d. 633) many
of the most devoted Moslems fell, the very men who knew
most Koran pieces by heart. 'Omar then began to fear
that the Koran might be entirely forgotten, and he induced
the CaUph Abubekr to undertake the collection of all it'?
parts. The CaUph laid the duty on Zaid, the son oi Zaid's
Thibit, a native of Jledina, then about twenty-two years of ''.''^'
age, who had often acted as amanuensis to the Prophet, "■'"'^°"
in whose service he is even said to have learned the Jewish
letters. The account of this collection of the Koran has
reached us in several substantiaUy identical forms, and
goes back to Zaid himself. According to it, he collected
the re^-elations from copies wTJtten on flat stones, pieces of
leather, ribs of palm-leaves (not palm-leaves themselves),
and such-like material, but chiefly "from the- breasts of
men," i.e. from their memory. From these he wrote a
fair copy, which he gave to Abiibeki-, from whom it came
to his successor 'Omar, who again bequeathed it to his
daughter Hafsa, one of the widows of the Prophet. This
redaction, commonly called al-sohof ("the leaves"), had
from the first no canonical authority; and its internal
arrangement can only be conjectm'ed.
The Moslems were as far as ever from possessing a uni-
form text of the Koran. The bravest of their warriors
sometimes knew deplorably little about it; distinction on thai
field they cheerfully accorded to pious men like Ibn Mas'ud.
It was inevitable, however, that discrepancies should emerge
between the texts of professed scholars, and as these men in
their several localities were authorities on the reading of
the Koran, quarrels began to break out between tlie levies
from diff'erent districts about the true form of the sacred
book. During a campaign in A.n. 30 (a.d. 650-1), Ho-
dhaifa, the victor in the great and decisive Imttle of Nebi-
wand — which was to the empirj of the SAsinids ■what
Gauganiela was to that of the Acli.-cmcnida; — perceived that
such disputes miglit become dangerous, and therefore urged
on the Caliph 'Othm.^n the necessity for a imiversally bind- 'O;!].
ing text. The matter was entrusted to Zaid, who had made :: 't^''
tho former collection, witli three leading Koraisliites. '^''*''-i
These brought together as many copies as they could lay
their hands on, and prepared an edition which w.is to bo
canonical for all Moslems. To prevent any further dis-
putes, they burned all 'Jii\ other ccdicis «;xcp,;}t that of
KORAN.]
M O H A Jvl M E D A N I S M
605
The
Kcraa
not com
plete.
Hafsa, which, however, was soon afterwards destroyed by
Merwin, the governor of Medina. The destruction of the
earlier codices was an irreparable loss to criticism ; but, for
the essentially political object of putting an ead to con-
troversies by admitting only one form of the common book
of religion and of law, this measure was necessary.
The result of these labours is in our hands ; as to how
they were conducted we have no trustworthy information,
tradition being here too much under the influence of dog-
matic presuppositions. The critical methods of a modern
scientific commission will not be expected of an age when
the highest literary education for an Arab consisted in
ability to read and write. It now seems to me highly
probable that this second redaction took this simple form :
Zaid read off from the codex which he had previously
written, and his associates, simultaneously or successively,
wrote one copy each to his dictation. It certainly cannot
have been by chance that, according to sure tradition, they
vrrote exactly four copies. Be that as it may, it is impos-
sible now to distinguish in the present form of the book
what belongs to the first redaction from what is due to
the second.
In the arrangement of the separate sections, a classifica-
tion according to contents was impracticable because of the
variety of subjects often dealt with in one siira. A chrono-
logical arrangement was out of the question, because the
chronology of the older pieces must have been imperfectly
known, and because in some cases passages of different
^ates had been joined together. Indeed, systematic prin-
ciples of this kind were altogether disregarded at that
period. The ])iece3 were accordingly arranged in indiscri-
minate order, the only rule observed being to place the
long silras first and the shorter towards the end, and even
that was far from strictly adhered to. The short opening
sura is so placod on account of its superiority to the rest,
and two magical formulse are kejit for a sort of protection
at the end ; these are the only special traces of design.
The combination of pieces of different origin may proceed
partly from the possessor^ of the codices from which Zaid
compiled his first complete copy, partly from Zaid himself.
The individual siiras are separated simply by the super-
scription— " In the name of God, the compassionate Com-
jMssioner," which is wanting only in the ninth. The
additional heading* found in our texts (the name of the
aura, the number of verses, etc.) were not in the original
codices, and form no integral part of the 'Koran.
It is said that 'OthmdTi directed Zaid and his associates,
in cases of disagreement, to follow the Koraish dialect ;
but, though well attested, this account can scarcely be
correct. The extremely primitive writing of those days
was quite incapable of rendering such minute differences
as can have existed between the jironunciation of Mecca
and that of Medina.
'OthmAn's Koran was not complete. Some jjassages are
evidently fragmentary ; and a few detached pieces are still
■ extant which were originally parts of the Koran, although
they have been omitted by Zaid. Amongst these are some
which there is no reason to suppose Mohammed desired to
suppress. Zaid may easily have overlooked a few stray
fragments, but that he purposely omitted anything which
he believed to belong to the Koran is veny unlikely. It
has been conjectured that in deference to his superiors he
kept out of the book the names of Jlohanimed's enemies,
if they or their families came afterwards to be respected.
But it must be remembered that it was never Mohammed's
practice to refer explicitly to contemporary persons and
affairs in the Koran. Only a single friend, his adopted
son Zaid (xxxiii. 37), and a single enemy, his uncle Abil
Lahab (cxi.) — and these for very special reasons — are men-
tioned by name ; and the name of the, latter has been left
in the Koran with a fearful curse annexed to it, although
his son had embraced Islam before the death of Mohammed.
So, on the other hand, there is no single verse or clause
which can be plausibly made out to be an interpolation by
Zaid at the instance of Abubekr, 'Omar, or "Othmdn. Slight
clerical errors there may have been, but the Koran of
"OthmAn contains none but genuine elements, — though
sometimes in very strange order.
Of the four exemplars of 'Othmans jvoran, one was kept;
in Medina, and one was sent to each of the three metro-j
politau cities, Cufa, Basra, and Damascus. It can still bo
pretty clearly shown in detail that these four codices
deviated from one another in points of orthography, in the
insertion or omission of a wa (" and "), and such-like
ni'nutise ; but these variations nowhere affect the sense.
Ail luter manuscripts are derived from these four originals.
At the szme time, the other forms of the Koran didOt'.;r
not at once become extinct. In particular we have '
some information about the codex of Obay. If the
list which gives the order of its siiras is correct, it must
have contained substantially the same materials as our text ;
in that case Obay must have used the original collection
of Zaid. The same is true of the codex of Ibn Mas'iid,
of which we have also a catalogue. It appears that the
principle of putting the longer suras" before the shorter wa3
more consistently carried out by him than by Zaid. He
omits i. and the magical formulae of cxiii. cxiv. Obay,
on the other hand, had embodied two additional short
prayers, which we may regard as Mohammed's. One
can easily understandthat differences of opinion may have
existed as to whether and how far formularies of this kind
belonged to the Koran. Some of the diverge"nt readings
of both these texts have been preserved, as well as a con-
siderable number of other ancient variants. Most of them
are decidedly inferior to the received readings, but some
are quite as good, and a few deserve preference
The only man who appears to have seriously opposed Ibc
the general introduction of 'OthmAn's text is Ibn Mas'ijJ. Miu'u'l.
He was one of the oldest disciples of the Prophet, and had
often rendered him personal service ; but he was a man of
contracted views, although he is one of the pillirs of Mos-
lem theology. His opposition had no effect. Now whicn
we consider that at that time there were many Moslems
who had heard the Koran from the mouth of the Prophet,
that other measures of the imbecile 'Othmin met Tvith
the most vehement resistance on the part of the bigoted
champions of the faith, that these were still further incited
against him by some of his ambitious old comrades until
at last they murdered him, and finally that in the civil
wars after his death the several parties were glad of any
pretext for branding their opponents as infidels ; — when
we consider all this, we must regard it as a strong testi-
mony in favour of "Othmin's Koran that no party, not
even that of 'Ali, found fault with his conduct in this
matter, or repudiated the text formed by Zaid, who was
one of the most devoted adherents of "OthmAn and his
family.
But this redaction is not the dose of the textual history of the La' er
Koran. The ancient Arabic aljihabet was very imperfect ; it not bi. tor*
only wanted marks for the abort, and in part even for tlie long of *.'js
vowels, but it often expressed several consonants by tb> same sign. te^t.
Hence there were many words whicb could be read in very di/Tcrent
ways. This variety of possible readings was at first very fiieat, and
many readers seem to have actually made it tlieir object to discovler
pronunciations whicb were new, provided they were at all appro-
priate to the ambiguous text. There was also a dialectic license jn
grammatical forms, which bad not as yet been greatly restricted.
An effort was made by many to establish a more refined pionuncia.'
tion for the Koran than was usual in common life or in semilsr
literature. The various schools of "readers" differed very widely
from one another ; although for the most part there was no im-
portant divergence as to the sense of words. , A few of them grailb-
Manu-
scripts
ComirT*
«lly N>so to special authority, and the rest disappeared. Seven
reaJc-s are generally leclconed chief authorities, but for practical
purposes this number was continuaUy reduced in process of time ;
so that at present only two "reading-styles" are in actual use,—
the common style of Hafs, and that of Nafi', which prevails in
Afnca to the west of Egypt. There is, however, a veiy comprehen-
sive massoretic hterature in which a number pf other styles are indi-
cated, Iho invention of vowol-sigus, of diacritic points to dis-
tinguish similarly formed consonants, and of other orthographic
signs, soon put a stop to arbitrary conjectures on the part of the
readers. Many zealots objected to the introduction of these inno-
vations in the sacred text, but tlieological consistency had to yield
to practical necessity. In accurate codices, indeed, all such addi-
tions, as well as the titles of the sura, etc., are written in coloured
ink, while the black characters profess to represent exactly the
original of 'Othmdn. But there is probably no copy quite faithful
in this respect.
In European libraries, besides innumerable modem manuscripts
of the Koran, there are also codices, or fragments, of high anti.
gmty, some of them probably dating from the 1st century of the
!• light. For the restoration of the text, however, the works of
ancient scholars on its readings and modes of writing are more
impoitant^ than the manuscripts ; which, however elegantly they
may be -vvntten and ornamented, proceed from irresponsible copj-ists
The original, written by 'Othra.in himself, has indeed been exhibited
in various parts of the Mohammedan world. The library of the
India Office contains one such manuscript, bearing the subscription :
Written by Othmdn the son of 'AllViu." These, of course are
barefaced forgeries, although of very ancient date ; so are those
which profess to be from the baud of 'Ali, one of which is preserved
Sn the same library. In recent times the Koran has been often
printed and lithographed, both in the East and the West.
• Shortly after Mohammed's death certain individuals applied
themselves to the exposition of the Koran. Much of it was obscure
from the beginning, other sections were unintelligible apart from
a knowledge of the circumstances of their origin. Unfortunately,
those who took possession of this field were not Tery honourable!
Ibn 'Abbas, a cousin of Mohammed's, and the chief source of the
traditional exegesis of the Koran, has, on theological and otlier
grounds, given currency to a number of falsehoods ; and at least
some of his pupils have emulated his example. These earliest
expositions dealt more with the sense and connexion of wliole
verses than with the separate words. Afterwards, as the know-
ledge of the old language declined, and the study of philology
arose, more attention began to be paid to the explanation of
vocables. A good many fragments of this older theological and
philological exegesis have survived from the first two centuries of
the Flight, although we have no complete commentaiy of this
psnod. Most of the expository material will perhaps be found in
the very largo commentary of the celebrated Tabari (a.d. 839-923)
of which an almost complete copy is in the Viceregal library at
Cairo. Another very famous commentary is that of°Zamakhshari
(a.d. 1075-1144), edited by Nassau-Lees, Calcutta, 1859 ; but this
Bcholar, with his great insight and still gi-eater subtlety, is too
MOHAMMEDANISM
[KOEA:r.
apt to read his own scho.astic ideas mlo the Koran. The favourite
commentary of Baidawi {ob. a.d. 1286), edited by Fleischer
Leipsie, 1846-1318 is little more than an abridgment of Zamakh
shari s. 1 housands of commentaries on the Koran, some of them of
prodigious size, have been written by Moslems ; and even the num^>,T
of those still extant in manuscript is by no means smalL « Ithoi-"',
these works a 1 contain much that is useless or false, yet" thev ala
invaluable aids to our understanding of the sacred book. An un-
.I'ffr'l ff ""P'^" J\'",' "," '^""l''' ''" ""^-y "''"S^ ^' a glance moro
''ZJ-"'^V g™<l Jl°f?°> ^ '0 i^ under the iuliuence of religio,^
prejudice ; hut we should still be helpless without the exe-retVal
literature of the Mohammedans. Nevertheless, a great deal remains
to be accomplished by European scholarship for the correct inter!
pretatioii of the Koran. We want, for example, an cxhaustiva
classification and discussion of all the Jewisfc elements in tho
Koran ; a prai.scworthy beginning has already been made ia
Gcigers youthful essay : JFas hat Maho-nul om dm Judcnlhu.,1
avfgcnommcnt (Bonn, 1833). We want especially a thorouf-l.
commentary, executed mth the methods and resources of modern
of'l°'4;nJ'?- °E-*u l'"'S",^g^ " ^-ouW seem, can even boast Tr«u.
of a transktion which completely satisfies modem requirement... -^
The best are in English ; where we have the extremely pr.'a- ^^'
phra^tic, but for its time admirable translation of Sale (repeatedly
printed), that of Eodwell (1361). which seeks to give tlie pieces in
chronological order, and that of Palmer (1880), wdio .wisely follow,
the traditional arrangements. The introduction which accompani- .
P.almers translation is not in all respects abreast of the most recei.;
seholarslup. Considerable extracts from the Koran are well trans-
lated m E. W. Lane's Selections from the Kur-dn
Besides commentaries on the whole Koran, or on special parti
and topics the Moslems possess a whole literature bearing on thi i-
sacred book There are works on the spelling and right pronun-
ciation of the Koran, works on the beauty of its language, on th-
number of its verses, words and letters, etc. ; nay, there are cve:-
works which would nowadays be called "historical and critical
introductions. Moreover, the origin of Arabic philology is inti-
mately connected with the recitation and exegesis of tlfe Koran
^r f 'tv," 'm ',"'P°'-l^"ee <,f the sacred book for the whole mental
ife of the Moslems would be simply to wite the history of that
lie Itself; for there is no department in which its all-pervadin<-
but unfortunately not always salutary infiucnce has not -been felt,
itJ.lL'' """.I, reverence of the Moslems for the Koran reaches Ete«,{y
Its climax m the dogma that this book, as the divine word, i c. .v the
inought, 13 immanent in God, and consequently rfcrnaZ and i^,,- Uc'^n
matexl Ihat dogma has been accepted bv almost all Mohammed,-i-s
since the beginning of the 3d century. Some theologians did
indeed protest against it with great energy ; it was in fact too pre-
posterous to declare that a book composed of unstable words and
letters, and full of variants, was absolutely divine. But what were
the distinctions and sophisms of the theologians for, if they could not
remove such contradictions, and convict their opponents of heresy ?
The followiiiK works may be specially consulted : Weil, Binhiluna in dn
*w. 11-., ^v*cii., J3IO, III. viUKiQKe, uescnicJiucus I
tJie Lives of Mohammed by Muii- and Sprenger.
(Ta K.)
Abbas, 551, 574 ; honsc
of, 574 sq.
AhhfLsid aj-nasty, 57S-
6Sf>,
•Abd al-Melik, 5C9.
Abderamc, 575, 570 sq.
Abiibekr, 548, 561 sq.
Abu eanlfa, 595.
Abu '1-' Abbas, 577 53.
Abu Lahab, 550.
Abii Mosliin, 576, 578.
Abu Talib, 546, 643, 549.
Africa conquered, 607,
672:
:volf:
A"hlfibitcs, 579, 587.
'Aif, 643, 5G3, 506 ; houao
of, 574, 579, 5S4.
Amin, 583.
Amir al-OirtfirA, 687.
•Amr b. aX-'Ati (Amron),
553, 565, 507.
Arab heathenism, 640.
Ash'ari, 593.
Assagiiins, 594.
liagbdid founded, 679.
Banu Kainoki, 565.
Jianu Nadfr,'650.
Eannccid'es, 581.
Ba.?ni. 562, 590; BChool
of. "'"
Bokhdri, 665.
Buyid dynasty, 5S7, 588.
Cadi, 591.
Caliph, 561, 589, 591.
Canuatliians, 586, 504.
Commerce, 597.
Ctesiphon, 562.
Cufa(Kula), 664, 670, &c.
Vahhak, 669.
" D'efendei-s " (An^dr), 554.
Dlwan, 689. 591.
Duiiiat al-Jandal, 5C5.
"Emigrants"(Mohd)Lriii),
554, 563.
Fill ma, 546.
Fiiiimitos, 68"
Faira, 548,
Intjex.
, 504.
Fosse' Waroftho, 551J.
Olixssan, 645, bdZ.
Grammarians, 595.
Greeks, wars with, 567,
570, 572, 574, 580, 6Si',
584, '58j.
Hidi 581.
HiOJM. 509, sn Sfjtj.
IJamdinite dynasty ES7.
pamza, 550, 556.
Uanifs, 547.
HArun al-Rashid, SSL
pasan b. 'AH, 500.
Uiishimitcs, 645.
Hcgira. See Hijra.
H.eromax (battle), 5C2.
Rijra, 545, 651.
llira, 645, 662.
Hird, Alt., 547.
Historians, 696.
Hodaibiya (treaty), 657.
Hosain b. 'All, 567.
"Hypocrites," 554.
Ibn al-AsIi'ath, 572.
Ibn panbal, 684, 595.
Ibn Mas'iid, 601.
Ibn Obay, 552, 554.
Ibn Zobair, 507, 608, 670
sqq.
Ibrahim (Caliph), 576.
Ikhshldites, 6S7.
Imdms, 592 ; of house of
,;Ali, 593.
'Isd b. Musd, 579*7
Ishim, 647 ; chief pre-
cepts, 553
, 693.
Jabarites,
Ja'far, 581, 582.
547, 550, 652, 653,
Ji'ri'ina, 659.
Kadaritca, 692,
KAdisIya (battle), 562.
Kerbela (battle), 563.
Khadija, 646, 643, 55a
Khaibar, 652, 557 sq.
Khdlid, 658, 562.
Khdrijit«s, 560, 504, 665,
569, 571, 692.
Koraish, 545, 559, 663.
Koran, 697-606.
Korai?a, 550.
kotaiba b. Moslim, 5"3,
674.
Uw, 594.
Mahdi (Caliph), 580; Mo-
hammed tlie, 679.
Malatiya, 579.
Malik b. Anas, 505, 693,
694.
Ma'miin, 583.
Mauaiir, 578 sq.
Mai-tel, Charles, 576^
Maslama, 574, 670.
Mecca, 645 sqq., 659, 669,
Mo'd>viya I., 563, 506 sq.i
M. II., 560.
Mohallab, 569 gqq.
Mokhtdr, 5CS sqn.
Money, 672, 51iO.*
Monta?ir, 5Sj.
Moslim b. 'OK-ba, 668.
Mosta'in. 5S5.
Mo'tasim. 684.
Mo'tamid, 6S6.
Motawakkil, 5S5,
, 692.
Mo-t
Mu ^.
Xeh.'uvend (battle), 562.
Obaid All.'ili, 608.
Obay, OOJ.
Ohod (battle), 556.
"Oivba, 507.
■Omar I., 650, 563: *0. 11-,
574.
Oniaj-j'Rds, 645, 500. 563
dynasty, 565-576 ; in
Srain, 579.
Orthodox sects, 593.
'Othmdn, 548, 549, 663;
Koran, 605.
Poets, 695.
l*rovinces, 593.
Ramai.tan, 55:i.
Pdwandi sect. 579.
689.
Rcve..„v.., .«...
Saffdrid (ij-na8t\', 586.
Samarkand, 507.
Science, 596.
Siffin (b.ittlc), 664.
Shdfi'f, 695.
Shi'ites, 504, 6CSL
Solaimdn, 574.
Sorra-man-ra'd, 5S5.
Spain conquered, 573 ; Cl ■
iiphate, 579.
Siifism, 694.
Sunna, 553, 594,
Tabiik, 661.
a'jiif, 545, 550, 559, 500.
'I'drik. 673.
Thco'logj', 592.
Trn.liUon (yadtth). 664.
594.
Tuh\nid dj-nasty, 680.
Wiikidi, 501, 596.
^ahd I., 573; W. II.,
Wdthik. 5S5.
Yahvft b. Al.dalliih, 6S2.
Y.izid I.. 667 «.; Y. If,.
575; Y. III., 570; Y. b.
Mohallab, 574, 675.
Zaid a *Ali, 575.
2iydd, 600, 507.
Bedr (battle), 655. Udshimites, 645. Snimwan; 667. '
Biodom Greek 7 or the Northmnborland burr. In a fe>, nam<» tlie coovcntiSiiTpe'Ss bSioi'^a Ke" naL^*?. ^SX' llH!: '■ folT^ =<'-of".s'uU
M O H — M O H
607
MOHL, Jules (1800-1876), Orientalist, was born at
Stuttgart 25th October 1 800, and educated for the Lutheran
Church at Tubingen ; but his inclinations carried him from
-.heology through Hebrew to Oriental studies, and in 1823
tie betook himself to Paris, at that time under De Sacy
the great European school of Eastern letters. He soon ac-
quired reputation, and from 1826 to 1833 was nominally
professor at Tubingen, with permission to continue his
jtudies in France, but he never entered on the duties of
this ofSce, Paris having become his second home. In
1826 he was charged by the French Government with the
preparation of an edition of the Sluih Ji'dmeh, the first
volume of which appeared in 1838, while the seventh and
last was left unfinished at his death ; in 1844 he was
nominated' to the Institut, and in 1847 he became pro-
fessor of Persian at the College de France. But his know-
ledge and interest extended to ail departments of Oriental
learning, and this catholicity of taste, united to a singular
impartiality of judgment and breadth of view, gave him a
quite remarkable personal influence on the course of East-
em learning in France. The chief sphere of this influence
was the Society Asiatique, which he served for many years
as secretary-adjunct, as secretary, and finally as president.
His annual reports on Oriental science, presented to the
society from 1840 to 1867, and collected after his death (4th
January 1876, at Paris) under the title Yingtsept Ansdes
£tudes Orientates (Paris, 1879), are an admirable history
of the progress of Eastern learning during these years, and
justify the high esteem in which he was held by scholars.
MOHLER, JoHANN A1..1M (1796-1838), Roman CathoUc
theologian; was born at the village of Igersheim in Wiir-
temberg on 6th May 1796, and, after studying philosophy
and theology in the Lyceum at Etlwangen, entered the
Wilhelmstift iu the university of Tubingen in 1817.
Ordained to the priesthood in 1819, he was appointed to
a curacy at Riedlingen, but speedily returned as " repetent "
to Tiibingen, where he became privat-docent in 1822, ex-
traordinary professor of theology in 1826, and ordinary in
1828. The controversies excited by his Symbolik (1832)
proved so unpleasant that in 1835 he accepted a call to
the university of Munich. In 1838 he was appointed to
the deanery of Wiirzburg, but died shortly afterwards
(12th April 1838).
MbUcr wrote bw Einkeit in dtr Kirche (Tubingen, 1825) ;
Athanasiut der Grosse u. d. Kirche seiner ZcU im Kampfe m. d.
Arianlsmus (2 voh., Mainz, 1827) ; Symbolilc, oder Darstellutig dcr
dorjmatischen Gegcnsdlzc der KathoKken u. ProteslarUen nach ihren
effmtlidicn Bclceiintiiisssdiri/lcn (Mainz, 1832 ; 8th cd., 1871-72 ;
Eng. transl. by J. B. Robertson, 1843) ; and Neue Untersuchiingcn
der Lekrgegcvsilx zwisckcn den, Katholikcn u. Protestantcn (1834).
His Oesammelte Schriflen «. AufMUe were edited by Dbllingor iu
1839 ; his Patrologic by Reithmayr, also in 1839 ; and a Biogra.jihie
by Woiner was published at Ratisbon in 1866. It is with the
Symbolik that his name is chiefly associated ; the interest excited
by it in Protestant cii-cles is shown by the fact that within two
years of its appearauce it had elicited three replies of considerable
miportancc, those namely of Caur, Marheiueke, and Xitzsch. But,
although characterized by abundant learning and acuteness, as well
as by considerable breadth of spiritual sympathy, and thus astimula-
tive and suggestive work, it cannot be said to have been accepted
by Catholics themselves as embodying an accurate objective view
of the actual doctrine of their church. The liberal school of
thought of which Mohler was a prominent exponent was dis-
couraged in official circles, while Protestants, on the other hand,
compfain th.it the author ias failed to grasp the vast signihcance
of the Reformation as a great movement in the spiritual history
of mankind, while expending needless pains on an exposition of
the doctrinal shortcomings, inconsistencies, and couti-auictions of
the individuals who were its leaders.
MOHR, Kakl Friedrich (1806-1879), a philosopher
whose greatest claims to scientific distinction are as yet,
though indubitable, only partially admitted, was the son
of a well-toJo druggist in Coblentz, and was bom 4th-
November 1 806. Being a delicate child, he received much
of.his early education at home, in great part iu his father's
laboratorj'. To this may be traced much of the skill ho
showed in devising instruments and methods of analysis
which are still in common use in chemical and pharmaceu-
tical laboratories. At the age of 21 he studied chemistry
under Gmelin, and, after five years spent in Heidelberg,
Berlin, and Bonn, returned with the degree of Ph.D. to join
his father's establishment. On the death of his father in
1840 he succeeded to the business, retiring from it for scien-
tific leisOTe in 1857. Serious pecuniary losses led him at
the age of 57 to become a privat-docent in Bonn, where he
was soon after appointed, by the direct influence of the
emperor, extraordinary professor of pharmacy. In pri-
vate and domestic life he was a man of singularly winning
manners, intensely fond of music and poetry, for the latter
of which he showed wonderful memory. But his uncom-
promising spirit — perhaps we might even in some cases
say his wrongheadedness — in matters of scientific and theo-
logical authority had raised such a host of enemies that
even royal influence could not secure his further advance-
ment. Although he stood at the very head of the scien-
tific pharmacists of Germany, his name was deliberately
omitted from the list of the commission entrusted with
the preparation of the Pharmacopoeia (Jermanica. Yet
in that work many of his ideas and processes w«re incor-
porated by the very men who had previously deuouiiccd
them. He died iu October 1879.
Mohr's best-known work is his Lchrbuch der chcmiseh-aimJijtisch-.i
TUrirjndhodc (1855), which has already run through many editions,
and which was specially commended by Liebie. His iniprovemenUi
in methods of chemical analysis occupy a long series of papei-s
extending over some fifty years. He also published a nuiuher of
physical papers on subjects such as Hail, St. Elmo's Fiie, Grouud-icc,
&c., and a curious notice of the earliest mention of Ozone. Ho
shows that Homer, ou four difi"erent occasions, mentions the sul-
Ehurous smell produced by lightning, and employs the very word
•om which the name of Ozone was long aftersvards coined. In
1866 appeared his Gcschichte dcr Erdc, cine Ocologie an/ iieucr
Grundlage, which has obtained a wide cii-culation.
But he will be remembered in future times mainly ou account of
a paper, Ueber die Aalur der IKarme, published in 1837, which
unfortunately has not yet appeared in full in an English translation.
The history of this paper is remarkable. It was refused admission
into Poggcndorff's Aii7talcn, and was then sent to Baumgartner of
Vienna, in whoso Zeitschrifl fUr Phtjsik, &c. , it was at once published.
-\s no proof-sheets reached Mohr, he concluded that his paper had
been lost or rejected, and contented himself with publishing a short
analysis in the Annalcn der Phetrmaciey of which he was an editor.
This analysis, it is only fair to say, though probably prepared by tho
author himself, gives a veiy inadequate idea of the scope and merit
of the paper. Iu 1864 Dr. Akin unearthed the paper from tho
forgotten pages of the Zcitschrift, and the author was enabled to
reprint it, with notes, while the recent discussions as to the history
of Conser\'ation of Energy were still being carried on. Along with
it he issued a number of other papcii* of gicatly inferior merit.
Unless Some still earlier anthor should be discovered, there can
be no doubt that Mohr is to be recognized as tho fii-st to enunriate
in its generality what we now call "conservation of energy." Tho
thesis of his paper must be stated in his own woi-ds, — " Besides
the 64 known chemical elements, there is in the physical world
one agent only, and this is. called Kraft (energy).' ft may appear,
according to circumstances, as motion, chemical affinity, cohesion,
electricity, light, and magnetism ; and from any one of theso
forms it can bo transformed into any of the others." Even now,
after nearly half a century of rapid advance in science, it would
be difficult to improve this statement except by inserting, as regaids
transformation of energy, some such guarding expression as "in
whole or in part." But if Mohr had inserted this, he might have
had claims to the "dissipation of energy ''also. Mohr's starting-point
appears to have been the discovery (by Forbes) of the polarization
of radiant heat. He ^oes through the whole o' the then range of
physics, pointing out the explanation of each experimental result as
a transformation of energy, mentioning even tfie electric currents
produced by electro-magnetic induction as a transformatioi of the
energy required to draw the coil fi-om the magnet — one of the earl'er
methods used by Joule for quantitative determinations. His nu-
merical results, based on data quoted from various books, arc, it is
' It is to be remembered tQ.at even the most accurate authorities in
Germany — as, for instance. You Helniholtz in his Essay of 1847 — used
till quite recently the word Kraft in the sense of Energy.
G03
M O i — M O L
true, very inaocuvnto ; Hie correct cXKi-imcntal cletorminations we
owe 'to Joule. But it mU3t be rememuered that these speculations,
^Jariii" as they were and accurate (on the whole) as they I'.avo been
found" to bo, required the contirmation which they received from the
••xlierimental work of Colding and Joule, or from the Sssatj of Von
lli-lmholtz, whoso basis also id wholly experimental, being the fact
that " perpetual motion " is recognized as unattainable.
MOIB, David Macbeth (1798-18S1), the "Delta" of
BliirlvoocTs Mazarine, one of its most popular contributors
in its early days, was "bom at Musselburgh 5th January
1798, and was a physician in active practice there from his
manhood to his death (6th JfJy 1851). He seems to have
been a man of winning manners and noble integrity of
character, and the intrinsic value of his poetry has been in
consequence somewhat over-estimated by critics of repute
who enjoyed his personal acquaintance. He had no inde-
pendent vein as a writer of serious verse, and his technical
■qualities as a poet do not bear examination. But liis verses
were luidoubtedly popular with the readers of the magazine
at the time. A collection of them was edited by Thomas
Aird in 1852. As a kindly humourist "Delta" had a more
original turn. His Antohioyraphy o/ Mansie Waucli, pub-
lished separately in 1828, is a Scotch classic. And some
of his satirical squibs on passing events were written with
great freshness and spirit. Has Outlines of the Ancient
History of Medicine (1831) evidence his industry and ver-
satility of talent. His Sl^etch of the poetical literature of
the past Half Century (1851) is more remarkable for the
grace of its rhetorical ornaments than for depth or fresh-
ness of insight._
MOIR, Geoege (1800-1870), author of the treatises on
" Poetry " and " Romance " in the seventh edition of the
Ihicyclopmlia Britannica, and born at Aberdeen in 1800,
•was an Edinburgh lawyer of very varied accomplishments.
He was appointed professor of rhetoric in 1835, professor
of Scots law in 1864 ; he had a considerable success at the
Scottish Bar, was successively sheriff of Rosa and sheriff
of Stirling, and was a frequent contributor to Blaclcwoo(ts
Magazine. Moir honourably maintained the literary tradi-
tions of Edinburgh law. He was a man of very wide
■reading, catholic sympathy, and fastidious taste, alive to
-very various degrees and kinds of excellence in literature,
but too critical and hard to please to do justice to his own
■wealth of ideas. He died in 1870.
MOISSAC, chief town of an arrondissement in the
department of Tarn-et-Garonne, France, is situated on the
right bank of the Tarn, and on the railway line from Bor-
deaux to Cette, 1 7 miles west-north-west of Montauban. The
church of St Peter, belonging to the 1 5th centuj-y, has a
doorway of the 12th century, remarkoble for its elaborate
and beautiful sculpture, representing Scriptural scenes.
Connected with the choir of the church is a cloister dating
from the beginning of the 12th century, and one of the
finest specimens of this kind of building in France ; the
pointed arches are supported by small columns with
sculptured capitals. The town has a large trade in com
and flour, and the-mills afford employment to a considerable
number of persons. The population in 1881 was 9202.
Tlie town owes its origin to an abbey founded between 630
and 640 by St Amand, the friend of Dagobert. After being
devastated by the Saracens, the abbey was restored by I^ouis of
Aquitaine, eon of Charlemagne. Subsequently it was made de-
pendent on Cluny, biit in 1618 it was secularized by Pope Paul
v., and replaced by a house of Aiigustinian monks, wduch was
suppressed at the Revolution. The town, which was erected into
a commune in the 13th century, was taken by Richard Coour do
Lion, uud by Simon de Montfort
MOKADDASl Shams al-D(n Abu AbdallAh Molmm-
med ibn Ahmad al-Moljaddasf, i.e., of Jerusalem, also called
al-Bash-'liarl, was the author of a famous description of the
lands of Islam, which much surpasses the earlier worlcs of
the same kind. His paternal grandfather was an architect
of eminence, who con.strnotccl many public works in Pales-
tine, and his mother's family was opulent. Ho was himself
a v/cll-educated and talented man, with an .exorbitant idea
of his ov.n qualities, and some curious affectations, such as
that of imitating for each region the dialect of its inhabit-
ants. His descriptions rest on very extensive travels
continued through a long series of years. His first pilgrim-
age was made at the age of twenty, but his book was not
published till a.h. 375 (985-6 a.d.), when he was forty
years old. The two MSS. (at Berlin and Constantinople)
represent a later recension (a.h. 378). The book became
known in Europe through the copy brought from India
by Sprenger, and was edited by De Goeje in 1877 as the
third part of his Bihlioih. Geographorum Arahicorum.
MOKANNA l^Al-Mokanna^, "the veiled") was, as
explained above, p. 580, the surname given to Hakim, or
'Ati, a man of unknown parentage, originally a fuller in
Merv, who posed as ah incamation of Deity, and headed
a revolt in Ivhorisin against the caliph Mahdi. Much is
related of his magical arts, especially of a moonlike light
visible for ati enormous distance which he made to rise from
a pit near Kaklishab. He died by poison in a.h. 163
(779-80 A.D.).
JIOKSHAN, a town of Russia, situated in the govern-
ment of Penza, 27 miles to the north-west of the capital of
the province, and 1 8 miles from the Ranzay railway station.
It has HjSOO inhabitants, who are engaged in agriculture,
or work in flour-mills, oil-works, tanneries, and potash-
works. A few merchants export corn and flour. Mokshan,
which was built in 1535 as a fort to protect the coimtry
from the raids of the Tatars and Kalmuks, is suppos-2d
to occupy the site of the town of Mescheryaks, Murundra,
mentioned as early as the 9th century. It has begun
rapidly to increase since the railway between Moscow aiid
Penza was made.
MOLA, or MoLA di Baei, a seaport tc■^^•n of Italy, in the
province of Bari, 13 miles from Bari on the railway to
Brindisi. It is an old-fashioned place ■nith irregular streets,
but outside of the walls several new districts have groiMi
up. The foreign, and to some extent also the coasting,
trade has considerably declined since 1863, and the com-
munal population has decreased from 12,574 in 1861 to
12,435 in 1881. Little is known about the early history
of Mola ; it was sold by Alphonso I. to Landolfo Maramoldo
in 1436, and ten years afterwards to Niocolo Tovaldo.
MOIASSES. See Sugar.
MOLAY, Jacques de, a native of Biu'gundy, becams
grand-master of the order of the Temple in 1298, and
was the last who held that dignity. He was burned at the
stake in 1314. See Teitplars.
MOLDAVIA. See Rouii.iJiiA
MOLE (contracted form of mould-warp, i.e., mould-
caster), a term restricted in England to the common mole
{Talpa europxa), a small, soft-furred, burrowing mamma),
%vith minute eyes, and broad fossorial fore feet, belonging
to the order Jnsectivora and family TalpiJa; but generally
applied elsewhere to any underground burrowing animal
of the class ilammalia. Thus, in North America we find,
representing the same family, the star-nosed moles {Con-
dylura), and the shrew moles {Scalops and Scapamis) ; in
Souti Africa, the golden moles of the far-removed family
Chrysochlotidx ; and in South-East Europe, Asia, and
South Africa, the rhizophagous rodent moles of the order
Rodcntia and families Spalacidx and Miiridx (see Mam-
malia, vol. XV. pp. 405, 419, figs. 64 and 96).
Talpa curopma, the Common Mole, type oi the genus
Talpa,^ is about six inches in length, of which the tail
measures somewhat more than an inch ; the body is long
* Ei^ht species may be recognized, and i
dentition, as follows : —
ngod, according to tlieir
MOLE
609
»nd cylindrical, and, owing to tlie very anterior position of
the forelimbs, the head appears to rest between the
shoulders; the muzzle is long and obtusely pointed, ter-
minated by the nostrils, which are close together in front ;
the minute eye is almost hidden by the frir ; the ear is
without a conch, opening on a level with the surrounding
integument ; the forelimbs are rather short and very mus-
cular, terminating in broad, naked, shovel-shaped feet, the
palms normally directed outwards, each with five subequal
digits armed with strong flattened claws ; the hind-feet, on
jthe contrary, are long and narrow, and the toes are provided
with' slender claws. The body is densely covered with
soft, erect, velvety fur,— the hairs uniform in length and
thictness, except on the muzzle and short taU, the former
having some straight vibrissas on its sides, whilst the
latter is clothed with longer and coarser hairs. The fur is.
generally black, with a more^or less greyish tinge, or
brownish -black, but various ipaler „ shades up to piu-e
white have been observed.
The food of the mole consists 'chiefly of the common
earth-worm, in pursuit of which it forms its weU-knpwn
underground excavations. Its habits, so difficult to observe,
were many years ago most patiently studied and described
by M. Henri le Court. Like many other mammals the
mole has a lair or fortress to which it may retire for
security. This is constructed with much ingenuity. It
consists of a central nest formed imder a hiUock which is
placed in some protected situation, as under a bank, or
between the roots of trees. The nest, which is lined with
dried grass or leaves, communicates with the main-run by
four passages, one of which only joins it directly, leading
downwards for a short distance and then ascending again ;
the other three are directed upwards and communicate at
regular intervals with a circular gaUeiy constructed in the
upper part of the hillock, which in turn communicates by
five passages leading downwards and outwards with another
much larger gallery placed lower down on a level with the
central nest, from which passages proceed outwards in
diSerent directions, one only communicating directly with
the main-run, while the others, curving rovmd, soon join,
or end in culs-de-sac. The main-run is somewhat wider
than the animal's body, its walls are smooth, and formed
of closely compressed earth, its depth varying according
to the nature of the soil, but ordinarily from four to six
inched Along this tunnel the animal passes backwards and
forwards several times daily, and here traps are laid by
mole-catchers for its capture. From the main-run numerous
passages are formed on each side, along which the animal
hunts its prey, throwing out the soil in the form of mole-
hills. The mole is the most voracious of mammals, and,
if deprived of food, is said to succumb in from ten to
twelve hoxirs. Almost any kind of flesh is eagerly devom-ed
by captive moles, which have been seen by various observers,
as if maddened by hunger, to attack animals nearly as
large as themselves, such as birds, lizards, frogs, and even
snakes ; toads, however, they will not touch, and no form
of vegetable food attracts their notice. If two moles be
confined together without food, the weaker is invariably
devoured by the stronger. They take readily to the water —
Sn this respect, as well as in external form, resembling their
{X.) i. I, c. J, pna. i, m. |
(B.) i. J, c. i, pm. I, pi. J
2 (r. Kogura).
2 (r. eitropsa, CBBcat longirostrU,
(C.l L 3, c. -J, prm. \, m.-f x 2 {T. Icucnira, Uptura).'
(D.) i. I, c. \, prm. |, m. J x 2 (T. moschata).
'E-^cept in T. europseOy the eyes are covered by a membrane."^- In
T. m-icmra the short tail is concealed by the fur. T. europsBa ex-
tends from Eb^land to Japan. T. cseca is found south of the Alps, the
remaining species are all Asiatic, and of them two only — T. micrura
and T. Uucrura — occur south of the Himalayas. (See Dobson, Mono-
graph ()flhe Insedivora, Part ii., 1883.)
representatives on the North American continent. Bruce,
writing in 1793, remarks that he saw a mole paddling
towards a small island in the Loch of Clunie, 180 yards
from land, on which he noticed molehills.
The sexes come together about the second week in
March, and the young — generally from four to six in
number — which are brought forth in about six weeks,'
quickly attain their full size.
Th« mole exhibits in its whole organization the most perfect'
adaptation to its peculiar mode of life. In the structure of the
skeleton very striking
departui'es fi-om the
typical mammalian
forms are noticeable.
The first sternal bone
is so much produced
anteriorly as to extend
forward as far as a
vertical line let down
from the second cervi-
cal vertebra, carrying
with it the very short
almost quadrate cla-
■yicles, wnich are arti-
culated with its an-
terior extremity and
distally with the hu-"
men, being also con-
nected ligamentously
with the scapulae. The
forelimbs are thus
brought opposite the
sides of the neck, and
from this position a
threefold adVautage is
derived : — in the first
place, as this is the
naiTowest part of the
body, they add but
little to the general
width, which, it in-
creased, would lessen
the power of move-
ment in a confined
space ; secondly, this
posirioa allows of a
longer forelimb than
would othei-wise be
possible, and so in-
creases its lever power;
and, thirdly, although
the entire limb is rela-
tively very short, its ,, , „ «
anterior position en- Skeleton of Mole x J (lower jaw removed td
ables the animal, when «'"'■" '>'^» <>' ^ku")-
burrowilie to thrust ^> calcaneum ; eft., clavicular artlcuiatioa of the
*i , °' ft humerus : cl., clavicle ; e.c, external condyle of hn-
the claws so lar tor- ^j^^, . ^^ j^^^ . yj^ ^.b^jj, . ^^ biciform bons
ward as to be in a line (radial sesamoid); ft, humerus; i.c, latemal condyle
with the end of the of humerus ; it, left iliac bouc ; i.p, ramus of the
Ttiu77li> thpitiiTinrtance ilium and pubis ; is., ischium ; l.d, ridge of insertion
muzzle, tneimportance „( i^tissimus dorsi muscle: U, lesser trochanter;
ot which 13 e^aaent.^ j^, manubrium Btemi ; o, fomtn hypapophysial 80-
Posteriorly, W'e find the samoid ossicle ; oi, olecranon ; p., pubic bone widely
hind limbs similarly separatedfrom that ofthe opposite aide; pa., patella;
, i. p *v p.m., ridge for insertion of pectoralis major muscle;
id out ot the ^,^ pectineal eminence; r, radius ;r6riirs.t rib ; <
icLuuYcu uut ux fciii. p(^ pectineal eminence; r, radius; rb, nrst no; e,
way by approximation plantar sesamoid ossicle corresponding to the radial
of the hip - ioints to sesamoid (OS falciform) In the manna ; »c., scapula ;
the centre line of the J;*-i^'"*'' "rtlculafaon ot the humerus ; (, tibu ;
body. This is effected '
by inward curvature of the innominate bones at the acetabula
to such an extent that they almost meet in the centre, while tha
pubic bones are widely separated behind. ^ The shortness of the
x„ ... most interesting to observe how, in the golden moles
{Cliryxochloridm) of South Africa, the necessary modifications of.Uia
corresponding parts of the body and limbs fitting them for fossorial
action and underground progression have been brought about in a
totally different manner. In them the manubrium sterai is l^ot
anteriorly elongated, neither are the clavicles shortened ; but this is
made up for by a deep hollowing out of the antero-lateral walls of the
thorai, the ribs in these parts and the sternum being convex inw,iTds,
the long clavicles have their distal extremities pushed forward, and the
concavities on the sides and inferior surface of the thorax lodje the
thick muscular arms. , .
'' In Jacobs's Talpw Europeie Analome (Jena, 1816) thispart of tna
pelvic -wall (marked ^< in the fig.) was identified with the symphysis
XYL — 77
610
M O L — M O L
forelimb is due to the humerus, ■which, like the clavicle, is so
much reduced in length as to present the appearance of a
flattened X-shaped bone, with prominent ridges aud deep depres-
sions for the aitachmeDts and origins of the powerful muscles
connected with it. Its proximal extremity presents two rounded
prominences : the smaller, the true head of the bone, articulates as
usual with the scapula ; the larger, which is really the external
tuberosity rounded off, forms a separate synovial joint with the end
of the clavicle. This double articulation gives to a naturally loose
joint the rigidity necessary to support the gieat lateral pressure
sustained by the forelimb in excavating. The forearm bones are
normal, but those of the forefeet are much flattened and laterally
expanded. The great width of the forefoot is also partly due to
the presence of a peculiar falciform bone, lying on the inner side of
the palm and articulating by its proximal extremity with the wrist.
Into the radial side and under surface of this bone is inserted a
tendon derived from that of the palmaris longus muscle, which,
acting upon it as an abductor, separates it fiom the side of the
palm, and so increases the width of the latter, at the same time
rendering the palmar integument tense.
The muscles acting on these remarkably modified limbs are all
homologous with those of the cursorial insectivora, differing only
in their relative development The tendon of the biceps traverses
a long osseous tunnel, formed by the great expansion of the margin
of the bicipital groove for the insertion of the large pectoralis major
muscle ; the anterior division of the latter muscle is unconnected
■with the sternum, extending across as a muscular band between the
humeri, and co-ordinating the motions of the forelimbs. The teres
major and latissimus dorsi muscle« are of immense size, probably
relatively larger than in. any other mammal, and are inserted to-
gether into the prominent ridge below the pectoral attachment ;
they are the principal agents in the excavating action of the limb.
The cervical muscles connecting the slender scapulae, and through
them the forelimbs, with the centre line of the neck and with the
occiput Are large, and the Ugamentum nuchae between them is
ossified (a3 in all true moles) ; the latter condition appears to bo
due to the jjrolopgation forwards of the sternum {described abovej,
preventing all flexion of the head downwards ; and, accordingly, tha
normal oflice of the ligament being lost, it ossifies, and so aSbrda a
more fixed point for the origins of the superficial cervical muscles.
The skull is long, with slender zygomatic arches ; the nasal bonr3
are strong and early become united, and in front of them the no£triJ:i
are continued fonvards in tubes foimed of thick cartilage, the ser-
tum between which becomes partially or wholly ossified beneath.
There are 7 cervical, 13 dorsal, 6 limibar, 6 sacral, and 10-12 caudal
vertebrae ; of the dorsal and lumbar there may be one vertebra
more or less. The sacral vertebrae are united by their greatly ex-
panded and laterally compressed spinous processes, and all the
others, with the exception of the cervical, are very closely and solidly
articulated together, so as to siipport the powerful propulsive zwi
fossorial actions of the limbs. Dentition : i. |, c. ■}, prm. ^, m. g,
X 2 = 44 teeth. The upper incisors are simple chisel-edged teeth ;
the canine is long and two-rooted ; then follow three subequal
conical premolars, and a fourth, much larger, and like a canine;
these are succeeded by three molars with "W -shaped cusps. In tha
lower jaw the three incisors on each side are slightly smaller, and
slant more forwards ; close behind them is a tooth which, though
quite like them, must, from its position in fiontof the upper canines
when the jaws are closed, be considered as the canine ; behind it,
but separated by an interval, ia a large double-rooted conical tooth,
the first premolar ; the three following premolars are like the corre-
sponding teeth above, but smaller, and are succeeded, as above,
by three molars.
The geographical distribution of the common mole may be said
to exceed that of all the other known species of the genus to whidi
it belongs taken together. It extends from England to Japan,
and from the Dovre-Fjeld Mountains in Scandinavia and the Middle
Dwina region in Russia to southcra Europe and the southern slopes
of the Himalayas, where it occurs at an -elevation of 10,000 feet.
In Great Britain it is found as far north as Caithness, but in Ireland,
and in the Western Isles of Scotland (except Mull) it is altogether
unknown. (G. E. D.)
MOLECULE
IN the conception of the atomic as opposed to the con-
tinuous and infinitely divisible constitution of matter,
it is supposed that portions of matter called atoms exist,
.■which are separated, or are capable of being separated, from
«ach other by empty space. (See Atom). It may be the
case th t each atom has unchangeable shape and volume
as well as unchangeable mass, but such a conception of
an atom is not essential to the hypothesis. It is not even
necessary, as explained in the article Atom (voL iii., pp.
37, 38), to maintain that no part of space can be in two
atoms at the same time. But one attribute of the atom
npon which its permanence, or, so to speak, its personal
identity, depends, is its Constituent mass, and this remains
the same, unchanged and unchangeable, through all time.
Boscovich, indeed, goes so far as to regard the atom as
a mere centre of force, the result of whose existence is that
no two atoms or centres can approach each other within a
certain distance, while other physicists regard the atomic
Tolume as a distinct portion of space occupied by that
atom to the exclusion of every other, and comprising
within it matter ideally infinitely divisible, but the parts
of which in fact never have been, and never can be,
Steparated from each other. In this latter mode of viewing
the subject, all the conclusions of mechanics which are
based on the conception of the continuity and infinite divi-
pibility of matter may be applied to the equiUbriimi or
motion of each individual atom, the atomic theory merely
introducing the additional hypothesis that, in fact, these per-
sistent entities called atoms do exist, and that out of them
all substances which affect our senses are constructed.
tlhe theory of universal gravitation requires us to believe
in the existence of forces or actions between every portion
pubis, whcreos the true pubic bones are widely separated (as ehowu at
jp). In this miatako ho has been followed by most comparative anato-
mists ; and hence the mole is generally believed to present the unique
peculiarity that the outlets of the urinary, gooetiltivo, and digestive
organs do not pass through the arch of the pelvis.
of matter and every other portion, determinate in magni-
tude and direction, and such that, when on the infinitely
divisible hypothesis the volumes of these portions are
indefinitely diminished, these mutual forces are inversely
proportional to the square of the distance between the por-
tions (the distance between any two points, one in the
volume of each portion, being in this case taken as tha
distance between the portions), and directly proportional
to the products of the masses, or quantities of the two
portions of matter, — such forces being regarded provision-
ally as ultimate facts, while inviting fiu'ther analysis and
explanation. Chemical and chemico-physical investigations
indicate the existence of other actions between portions of
matter, following other and for the most part unknown
laws, and rapidly becoming inappreciable as the distance
between the reacting portions is increased. All theee
hypotheses are to be retained on the hypothesis of discrete
atoms as above enunciated, the mutual actions between
atoms being the resultant of the actions between the various
portions of their constituent matter. The volumes of the
atoms are so small that, for any sensible distances apart,
the line of the resultant mutual action between them may
be taken as coincident with the line joining any point in
the volume of one to any point in the volume of the other,
but, for distances or parts comparable with the linear
dimensions of the atoms, the size and shape of their bound-
ing surfaces must be taken into consideration, and perhaps
also the law of distribution of their constituent matter
within that surface. In all respects, unless we accept the
Boscovichian hypothesis, we simply regard the atom as
made up, so to speak, of infinitely divisible matter, while
substances, as we know them, are built up of indestrucliblo
and unchangeable atoms.
With this conception of an atom, as thus explained; wa
might be content to rest, confessing our total ignorance ol
the mode in which such atoms are built up into actual
substances, being satisfied to regard such substances as
MOLECULE
611
composed of these distinct portions of matter separated, or
capable of being separated, by empty space fk-om other
portions. But the iaolemdar hypothesis of the constitution
of different kinds of substances aims at analysing this
process by which such substances are built up out of their
constituent atoms. The molecule of any substance is, by
some chemists, defined as being the smallest portion of that
Bubstance to, which can be attributed all the chemical pro-
perties of the substance ; by others, as the smallest portion
which, so loag as the substance is chemically unchanged,
keeps together without complete separation of its parts.
In the langiuge of Clausius's theorem, if the parts of the
molecule have internal motion, the Hnetic energy of such
internal motion is equal to the virial of the mutual attrac-
tive forces of the parts. Thus the formation of the mole-
cule of each particular substance is viewed as an essential
step in the process of buOding up that substance out of
its constituent atoms. The molecule is first bmlt up out
of atoms arranged in its formation according to a definite
type, and then the substance itself is constituted of these
molecules. Of course molecules may be, and in fact in
many particular substances are, supposed to be mou-
atomic ; that is to say, the intermediate step of building
np the molecule out of the atoms has, in these particular
substances, been omitted, the atoms and molecules becom-
ing then identical. The particular arrangement of the
formed molecules in the building up of the substance de-
termines the physical state of that substance, — that is,
its fluid, solid, gaseous, crystalline, or amorphous state;
but the chemical properties of the substance depend upon
the constitution of the molecule. As the investigations
and theories of chemistry appear to indicate irresistibly
the existence of permanent atoms, so do they also lead
almost as necessarily to the conception of the molecule
as an entity which bears the same relation to special
substances that the atoms bear to matter generally. So
long as the molecule endures, the substance of which it
is the molecule retains its chemical properties ; with the
dissolution of the molecule, the substance, as that special
substance, perishes ; the atoms alone continue, and are free
to enter into other combinations. The permanence of the
molecule is relative, that of the atom absolute. This con-
ception of the molecular constitution of substances sug-
gests physical questions of great interest, such as the shape,
volume, and mass of the constituent molecules, and the
relative motions of which their parts are susceptible ; and
the answers to these questions cannot fail to be of great
value in chemical and chemico-physical investigations, as
well as in the theories of light and electricity.
Now, whatever differences may exist between the proper-
ties of difierent substances in the solid and liquid states,
there are certain properties which, in the gaseous state,
manifest themselves with no variation whatever in all sub-
stances alike. Hence the explanation of these common
properties — or gaseous laws, as they are called — ^has long
possessed a peculiar fascination for physicists. The tend-
ency to expand or fill all accessible space, manifested by
all gases, proves that on the molecular hypothesis their
compound atoms or molecules must be continually tending
to fly apart. We must conceive gases as constituted of mole-
cules, not Only separable but actually separated by space
void of the matter of which these gases consist ; and it may
be most reasonably expected, therefore, that any general
lavrs to which substances in this state conform may afford
us a valuable insight into the constitution of these separate
molecules.
Now the general laws to which all gases conform are :
(1) BoyWt law — that, in a given mass of any gas kept at
constant temperature, the pressure per unit of area upon
the cont^ining surface increases in the same proportion as
the volume occupied by the gas is diminished, or at least
with very slight deviation from exact proportionality ; (2)
Charles's law — that, if the temperature be varied while the
pressure upon the gas remains the same, the gas increases
hy TTid of its volume at zero centigrade for every degree
of centigrade added to the temperature, or, which in com-
bination with Boyle's law is the same thing, that if the
density be constant, the pressure is directly proportional to
the temperature measured from the point - 273° centigrade,
this point being called the zero of absolute temperature ;
(3) Avogadro's law — which asserts that aU gases at the
same temperature and pressure contain the same number of
molecules in the same volume ; and (4) Daltmi's law — that
in a mixture of different gases, when there is equilibrium,
each gas behaves as a vacuum to all the rest.
It was at one time considered that these phenomena
might be explained on the hypothesis of muttial repulsive
forces between the parts of which the gas is composed,
whether they were regarded as constituted of molecules or
of infinitely divisible continuous matter,"- but it has been
shown in the article Atom (vol iii. p. 39 sq.) that there
are at least two absolutely conclusive reasons why this ex-
planation cannot be accepted. These objections, together
with the experimental fact proved by Joule that gases, or at
any rate atmospheric air, expand into vacuum with scarcely
any appreciable change of temperature, must be considered
fatal to any mutual-force thtory of gaseous action, and,
accordingly, physicists have been driven to seek for other
methods of explaining these laws. The explanation which
has been more developed than any other is that known as
the kinetic theory of gases, which regards the intrinsic
energy of a gaseous mass as residing, not in the potential
energy of intermolecular forces, but mainly in the kinetic
energy of the molecules themselves, which are assumed to
be in a state of continual relative velocity, admitting at
the same time a possible small intermolecular potential
energy, and it may be also an interatomic energy, between
the atoms of the individual molecules. That some such
persistent relative motion does exist in every gaseous masa
is evident from the rapidity with which odours penetrate
the stillest air where no breath of wind — that is, of absolute
motion of translation of the mass as a whole or any portion
of finite size — is perceptible. It becomes an interesting
question whether the laws of mechanics admit of a masa
thus constituted ever arriving at a state of permanence ;
that is to say, whether, consistently with the hypothesis of
infinite irregularities in the directions and magnitudes of:
velocities of individual molecules, there may be found anyf
properties of the mass in the aggregate which remain
^ An argument in favour of the molecular constitution of gases, to
which attention was first called by Professor Osborne Reynolds
(Memoir '* On some Dimensional Properties of Matter in the Gaseous
State," PhU. Trans.^ 1879), is derived from certain phenomena
observed in highly-rarefied gases, and in the transpiration of gases
through porous plates. If, according to this argument, we hrvd in a
gas ta do with a continuous plenum, such that every portion must
possess the same properties, then these properties must exist inde-
pendently of the amount of gas contained in any space, although
their sensible effects might be increased or diminished by a variation
in that amount. If, then, we can find properties of a gas depending
on the size of the space in which it is enclosed, and on the quantity
of gas enclosed in this space, we have proof that gas is not continuous
— in other words, possesses dimensional structure. Such properties
we do find in highly-rarefied gases, as, for instance, in the pheno-
mena of Crooke's radiometer. The motion of the vanes when one
side is heated by incident rays appears to depend on the distance
between the vane and the containing walls of the vessel bearing some
not very high ratio to the distance between the particles or molecules
of the gas. At least no satisfactory explanation of the phenomena
consistent with the gas being continuous has yci been suggested.
Again, Professor O. Reynolds, from his experiments on the trans-
piration of gases through a porous plate, finds a relation between th»
gas and the coarseness or fineness of the plate, which would not exist
were the gas continuous.
612
MOLECULE
constant, and in agreement with the accepted laws common
to all gases. Now the physical theory of heat compels us
to regard the intrinsic energy of any gaseous mass as de-
pendent entirely or almost entirely upon the temperature.
If, therefore, this intrinsic energy is to be sought for in
the kinetic energy of the moving molecules, it follows
that the average value of the kinetic energy of the mole-
cules taken throughout the mass must be also a function
of the temperature.
We will proceed to investigate the condition of per-
manence of a number of molecules moving about irregu-
larly in any bounded space ; and, for simplicity's sake, we
shall first of all restrict ourselves to the case of monatomic
molecules.
We know nothing of the size or shape of these atoms,
except that the volume of each one must be incomparably
smaller than that of the containing region. In shape we
shall, as the simplest hypothesis, regard them as spherical.
We shall suppose that there are no iutermolecular forces
between any two such atoms, except of such a nature as
to be practically insensible when the atoms are not geo-
metrically in contact, and similarly as regards the forces
between the atoms and the material bounding surface,
such forces being of the nature called " conservative." So
that in point of fact we are investigating the mechanical
properties of an infinitely large number of infinitely small
and perfectly elastic spheres moving about in a given
region and subject to frequent collisions.
Problem. — A very large number of smooth elastic splieres, equal in
every respectf are in motion within a region of space of given volume,
and tkerefo: c occasionally impinge upon each other with various
degrees of relative velocity and in various relative directions; re-
qvired to find the law of distributimi of velocities in order thai such
distribution may be permanent.
Let N be the total number of spheres, and let
X(«.
'v) du dv dw
be the number of spheres whose component velocities, parallel to
the axes, are intermediate between u and u + du, v and v + dv,
w and w + dw respectively.
If c be the resultant velocity of any of these last-mentioned
spheres, and if # be the inclination of c to the axis of s, and 0 that
of the plane cz to the plane xz, the last-mentioned e^cpression will
become, by changes of the independent variables frofe x, y, z to
0, <p, and e,
X (", V, w) c- sin e de dtp de.
Let a spherical surface of radius unity be described about any
origin as centre, and let rfcr be written for the element sin e dd dtp
on this surface, then the last-written expression becomes
X [u, V, w) c- de da.
_ Since for the same magnikude of the resultant velocities all direc-
tions of motion must be equally probable, it follows that the co-
efficient of de da in the last-written expression must be a function
of c only, and therefore the number of spheres having component
velocities between u and u -f- dii., t. and d -h dv, w and w -H dw.
niust be
^ {e) du dv dw.
It is required to find the form of yUn order that the value of
this expression may be unaffected by collisions. The solution is,
that the number of spheres with component velocities between the
limits M iniu + du, v and v + dv, w and w + dw must be
Ae-'"^ dudvdw;
<"• Ae->''\^ dc d<r,
cmplojang tlio notation already used.
Integrating with respect to d<i from 0 to ir, wo find for the
mimber of spheres with velocities between cMiic + dc the expression
4w Ae
'de.
.^gain, since the number with component velocities betfreen u
and u + du, tiand v + dv, w and w + dw is
Ae-''('^ + o' + <"'^dudvdu>,
or (VA-e-'"''dU.) (yZ«-»"»di,) (VAe-'^<"'-dw).
it fol'owa that the number of spheres having velocities intermediate
be'wocn « and u + du parallel to the x azia is
•^ duj e - '"'- dvj
' dw.
du.
where A is to be determined by the equations
^A^ e-''-' du=N,
^Tr=^:
therefore
A =
that is to say, the number of sphered having velocities between c an!
c + dcia
\/ir
Multiplying this expression by c, and integrating the product with
regard to c from 0 to oo , and dividing by N, the mean velocity for
all the spheres becomes
2
and multiplying by c- instead of by c, we find the mean square of all
the velocities to be
Z_
2/t'
In the preceding investigation no account has been taken of
collisions between the spheres and the enclosing boundary of th^
region in which they are contained, because in every such collision
the magnitude of the velocity of each sphere is unaltered and its
direction is changed according to the ordinary law of reflexion,
whence it is evident that the distribution ia unaffected by sulIi
collisions. Also, the investigation has been confined to the cases
of spTieres colliding in paii-s, but since there need be no limit to
the smallness of the interval between any pair of collisions th^
result really embraces the cases of simultaneous collisions betwe/'O
three or more spheres ; for if a sphere A collides with another JJ,
and immediately afterwards with a third C, the resultant velocity
of A after this second collision must be the same as if it had col-
lided with B and C simultaneously.
The foregoing investigation has been given In some detail because
the principles upon which it proceeds are essentially the same as
those by which all questions of the distribution of energy among A
great number of mo\'ing bodies are determined, althougii it may be
found, as well as the detailed investigations of the results imme-
diately following, in published memoirs and systematic treatises oa
the kinetic theory of gases.
If the spheres be not all of equal mass, but if there be within the
region N spheres of mass m, N^ of mass m', and so on, then it may
be proved, by reasoning exactly similar to the foregoing, that when
the permanent or stable state of motion has been attained the
number of spheres of the N set with component velocities between
u and u + du, v and v + dv, w and w-\-dio vi
Amc2
Ac 2 dii, dv dw,
and the number of the N' set having component velocities betR'cen
u' and u' + du', ^ and i/ + rfy', w and vf -^dvf, is
where ^ — xi^-vv^-Vv?, c'^
for both sets, and
dxi dif du/,
v'^ + w'^, 7i is a constant the tzv.
^ ^r V 2 ; '
m
and so on if there be any other sets.
The mean veloftity and mean square velocity of each sphere of tl."
N set are
_?^ / ^ and — r respectively,
ard the moan kinetic energy of each of such spheres is
3^
2A'
the last result being common to all the set.^.
If the spheres in the given region be acted on by anf given forces
tending to fixed centres, and functions of the distances of the centivs
of the spheres from the centres of force, we may not in such r.iss
a.ssume, a priori, that the chances of velocities in all directions aic
the same ; but wo mav assume that the number of spheres of anv
set (N) with coordiiiatos of their oontrcs intonncdiate betiT";''
MOLECULE
613
asandaj+rfx, y and y+dy, s and z + dz, and component velocities
intarmediate between u and u + du^ v and v + dv, 10 and w+dzOf is
f (x, y, z, n, V, w) dx dy dz du dv dw.
In tlie state of permanence the form of ^ mnst be independent
of the time (t), so long as the sphere is moving free from jeollisions
with any other.
From the last-mentioned condition it must follow that, if ^i = «i,
^, = a.^ &c., be any equations among the variables determining the
position and motion of anj' sphere obtained by the elimination of t
from the equations of motion of that sphere, then ^f* must be of the
form ^ (01, 0-2, &c.). 'VTith the assumption, tlien, that the number of
spheres of the given set with variables bet^veea the above-mentioned
limits is
we find for the form of \p, by reasoning like the foregoing,
Ae~ ^^■*'~2~/, where % is the potential energy of the sphere in
tlie position x, y, z, and c^=w^-t-v^-J-w^, and A is a constant, the
same for all the sets.
If we integrate the expression Ae~ ^ - ^dx dy dz du dv dw
for all values of x, y, z within the given region, we find for the
r.umber of spheres of any set with component velocities between
XL and tt+dw, v and v-^dv, w and w-^dw,
Be' 2 du dv dw,
r; hence we easily see that the chances of velc:ities in aU directions
are the same, and that the mean velocity and mean square velocity
of any sphere of this set are — - — and — ^ respectively, andthemean
kinetic energy of any such sphere is ^, and therefore the same for
i\l the se
Furthermore, if we integrate the expressio^i
Ae~^ (X+ ~2'^dx dy dz du dv dw \
lor all values of «, v, and w from -00 to + « respectively, we
obtain a result of the fonn Ce ' ^^ dx dy dz, and therefore the number
of spheres of the set in question with centres within the elementary
volume dx dy dz, or, what is the same thing with the exception of a
constant factor, the chance of the centre of any sphere of that set
being within that elementary volume, is Ce~^^ dx dy dz, so that the
density of the JVset of matter in the neighbourhood of the point x, y,
z is mCe'^K
We are now in a position to compare the physical properties of a
medium composed of monatomic molecules in motion, and free
from any intermolecular or interatomic forces with those of ordiaarv
gasos, so long at least as the atoms are spherical.
Consider two contiguous portions of such a medium separated by
any plane parallel to that of yz, and, since the distribution and
motion of each set of spheres is independent of all the other sets,
let ua confine our attention to the spheres of the N set. Suppose
that there are N such spheres per unit volume in the neighbour-
hood of the point x, y, z, whose component velocities parallel to
the axis of x are between u and u + du. The number of these
spheres which cross the elementary area dy dz in time dt will be
the same as the number of the dH spheres whose centres are
situated within the elementaiy parallelepiped dx dy dz, in which
dz is equal to udt, and this number is
Xu dy dz dt.
Each of these spheres carries across with it a momentum parallel
to X equal to mu ; the total momentum parallel to x transferred
across dy dz in time dt is therefore
m2\^u^ dy dz dt.
If 1* be positive, this is positive momentum transferred from the
negative to the positive side of the plane y z ; and if u be negative,
this is negative momentum similarly transferred from the positive
to the negative side of that plane. In either case it follows that
by the mere motion of these spheres across the area dy dz the
positive momentum parallel to tne axis of a; is diminished by the
quantity inA'u* dy de dt on the negative side of the plane y z,
and increased^ by the same quantity on the positive side of that
plane in the time dt ; m being, as before, the mass of each sphere.
Hence, on the whole, there is a transference of positive x momentum
in the time dt across the area dydzeaualio mdy dz dt S u-N ; that
is, equal to ""
dy dz dt pu^,
where p is the density of the N matter at the point .r, y, z, and IJ^
is the mean square of the x velocities.
Bat either by int'^gration or general reasoning it is easily seen
that u^=z — , where v* is the mean sqnaro of the resultant velo-
cities of the i\^ spheres, and is equal, aJs we have proved, to
Therefore, there is a transference of positive momon^im fi-om the
negative to the positive side of the plane y z across the area dydz ia
time dt equal to
p dy dz dt
mh
Each separate sphere whose component velocities are u, v, and m
carries across the same area y and 2 momenta equal to mv and mw
respectively, so that in the time dt there are carried across the area
dy dz y and z momenta equal to Zmuv dy dz dt and 'Zmuw dy dz dt,
respectively. By symmetry it is clear that T-muv and "Zmuw are
separately zero. Therefore, the resultant mutual actions of the two
portions of the medium under consideration in the time dt is the
transference across the elementary area dy dz of a quantity of x
momentum equal to pdy dz dt -^ fr'om the negative to the positive
side of the bounding plane. If this mutual action, or, as it is gener-
ally called, "pressure" when referred to unit of-sudace, be danoted
by the ^mbol j?, we get the equation
p dy dz dt = p dy dz dt — ,
Since the momenta parallel to y and s remain unaltered, it
follows that the mutual action or pressure between contiguous por-;
tions of the medium in the neighbourhood of any point is normiil
to the hounding surface at that point. Since also the expression
for p or -^ is independent of the direction of the x axis, it fol'
lows that the pressure at any point of the medium is the same in
all directions.
If the contiguous portions of the medium be separated by a
material instead of an ideal plane, it wiU be necessary for the main-
tenance of equilibrium that there should be an action between this
plane and the adjacent medium, equivaldct to the transference of
momentum estimated above ; but action measured by the rate per
unit of time at which momentum is generated constitutes moving
force or statical pressure. Hence the force or pressure between the
plane and medium is normal to the piano, independent of the
direction of the plane through the point, and equal to the value of
-2j- at the point.
■When several sets of spheres are present together In the region
under consideration, the distribution of the centres and of the
velocities of each set is, as we have seen, independent of the co-
existence of the other sets. If therefore p,, p», &c. , be the densities
of the matter of the different sets in the neighbourhood of the point
X, y, 2, and if ft, p,, &c., be the pressures at that point defined as
above, and if m-,, 7n„, &c, be the masses of the spheres of each of
the sets, and p the total pressure, we get
P=Pi + Pi + ^<!-
Hence we arrive at the following conclusions : — (1) there is one
physical quantity having the same value for every set of spheres —
namely, the mean kinetic energy of each sphere, or -^ ; let this
quantity be called t ; (2) the distribution of the positions and
'velocities of the spheres of each set is independent of the coexist-
ence of the remaining sets, and is in all respects the same as if that
particular set existed alone in the region considered ; (3) the
pressure at any point referred to unit of surface at any point of
the medium arising from the action of any one of the sets is ^^ p",
where p is the density of that particular set at the point in question,
and T is the physical quantity above referred to as common to all
the sets. . _
This third inference may be expanded into the following three
laws :— (a) if t be kept constant, then the pressure arising from
each set varies as the density of that set ; (^) if p bokept constant,
then the pressure from each set varies as r ; (7) if- the pressures
for all the sets be the same, then — is also the same, or the num-
ber of spheres per nnit volume is the same.
Now suppose there is a mixture of any number of gases in any
region ; when there is equilibrium there is one phvsical quantity,
namely, temperature, which is the same for all; the intrinsic
614
MOLECULE
energy of this mixture depends, as we know, upcm its temperature,
and the energy of these moving spheres is entirely kinetic, and may
ho ci nceived, therefore, to he a function of the mean vis viva. Let
us tV.jn assume that in this medium of moving spheres we have a
representation of a mass of gases, and that what is called the
t3mf 3rature of the gaseous mass is nothing else than the t or mean
Idnetic energy of each moving sphere. Then, with this assumption,
the three parts (a, /3, 7) of inference (3) above correspond to the
gaseous laws connected vrith the names of Boyle, Charles, and
Avogadro I'espectively, and inference (2) corresponds with the law
of Dalton concerning gaseous mixtures.
"We may also deduce the ordinary hydrostatical equations of
equilibrium from the formuke which we have obtained.
For, since these equauons give U3
we get
and similarly
u = -^, and pzzruBe
mh '^
■hX
pr/J^pZ,
where X, JT, and ^ are the component impressed forces, or the
negatives of the space variations of x along the coordinate axes.
So far, therefore, the physical properties of aperfect gas or mixture
of such gases correspond, in all respects, with tne physical properties
of a medium consisting of a set of elastic spheres, or of a mixture
of sets of such spheres, with the sole assumption that the physical
property termed Temperature, in the case of the gas, corresponds to,
or is represented by, the mean kinetic energy of each of the spheres,
and that each sphere represents the chemical atom.
There are, however, physical properties of gases which this theory
fails to explain. The most important of these is the ratio of the
specific heats at constant volume and constant temperatui'e respect-
ively. The specific heat of gas expanding while bemg heated under
a constant pressure is greater than that of gas heated with a con-
stant volume, as when it is contained in a rigid vessel, for the
obvious physical reason that in the former case a portion of the
heat is converted into mechanical work, namely, that performed by
the expansion under the constant pressure. This ratio of the specific
heat of gas under constant pressure to the specific heat with con-
stant volume has been determined for many gases with great ac-
curacy, chiefly from observations of the velocity of sound in such
gases, in which velocity the value of this ratio bears a very im-
portant part.
Now, ou the assumption of the gas being constituted of a number
of elastic spheres in rapid but irregular motion among each other,
and the physical property of temperature being represented or
measured by the mean vis viva of each sphere, the ratio of these
specific heats must be exactly 1^.
For, if V be the volume occupied by a unit of mass of this moving
sphere medium, and r the number of spheres to the unit mass, and
it /) be the density, it follows that
rm = pv = l.
Also we know that^, the pressure referred to \xait surface, is given
by the equation
2
■where r is the mean vis viva. If now r increase from t to r + 5r,
while V remains constant, the increase of intrinsic energy mu.st be,
fiom definition, tSt. Also if there be a similar change in t without
the re:-;triction of v being constant, but supposing p to bo constant,
there is external mechanical work performed equal to p5v, where
ho is the increase of volume. Also
^ 3 '
and therefore the whole energy required to bo supplied from without
must be in this caae
Or thfi ratio of the energies to be supplied from without, in order
that the mean vis viva of the moving sphere medium should be
increased by the same amount in the two cases respectively, becomes
2
— L, or n.
If therefore the gaseous mass bo adequately represented by the
moving'sphere medium, the ratio of the specific boats must be 1|.
MfTcury vapour is the only gas for which the ratio has so largo
a value as this. Several of the more permanent gases have the
rati J rqual to 1'408, while in others it falls as low as 1-26. The
vaiuc for mercury vapour, as determined by Kundt and Warburg
{Poggcndorff, clviL 353), is between 1 '695 and 1 "631, the mean of .11
the observations being somewhat under 1'6. If any value al .vo
1'6 be insisted on it will be impossible to retain the theon- -.s.
above enunciated. In point qf fact we may say, in anticipa ' :■.
of what has yet to come, that there is no modification of the kir _:
theory as hitherto treated which could give a higher value for '. .;■
ratio in question than 1^.
It follows from what has been proved that either all known g/: i
and vapours, except the vapour of mercury, and perhaps cadmi -.i,
must be polyatomic, or else that the attempts to- explain the coi t;-
tution of gases by the kinetic theory must be aoandoned. V'j
must therefore proceed further to investigate the physical 7 :n.
perties of a medium consisting of compound atoms or molecules
built up of atoms in any definite arrangement, such molecules b( jg
in a condition of irregular motion among themselves, such a£ ■.■, e
have supposed in the cases of the spherical atoms hitherto c -n-
sidered.
It will be observed, on reference to the cases of the spheres hithr 1 to
investigated, that, whether there be forces to fixed centres in act uu
on the medium or not, the chance of any sphere having the cooili-
natesofits centre and its component velocities between xanda:-h.>,
y and y + dy, z and z -f- rfs, u and u + du^ v and v + dv, w and w + d ic,
is proportional to e ~ ^dxdydz du dv rfw, where E is the total enerfy,
kinetic, and potential, of the sphere in the state of position aji
motion defined by a;, y, z, w, i', w.
We may generalize this proposition, and prove that when tae
sphere is replaced by a molecule of any shape and constitution, 00
as to be defined as to position and motion by r genemjized coonli-
nates^i.-.g^with their corresponding momenta j^i...^^ the chances of
the molecule having its defining variables between the limits q-^ a':'l
9i-^^Qi--Pr and jp^-f rf/),, or, what is the same thing, the number ui
such molecules at any time with variables thus umited, whether
there be forces to fixed centres or not, and whether interatomic
forces or intennolecular forces are or are not in action on the mole-
cular aggregate, is proportional to
e'^^rdqy,,dp^
where A is a constant, the same for all molecules, and E^ is flie
total energy, kinetic and potential, of the molecule in the free eta's
as to position and motion, the potential energy being that of the
fixed centre forces on the molecule, together with that of its inter-
atomic forces, in the given position.
The problem before us may be stated thus : —
A number of similar molecules possessing in the whole n degrees
of freedom, where n is very large, are in motion in a region of spec j
bounded by a material envelope, under the action either of fora s
to fixed centres (called external forces) or of forces between different
molecules and different parts of the same molecule, as well as bv
forces between the fixed boundary and the contained molecules, all
of them conservative, so that the total energy, kinetic and potential,
of the aggregate remains always the same ; it is required to find th«
chance of a group of any one or more molecules possessing in the
whole r degrees of freedom, defined by the coordinates ffj...^,, and
momenta Pi-.-Prt where r is small compared with n, having it»
variables between the limits g^ and gi+dq^...p^ andp^ + dp^
We might start with the assumption made above in the caso ot
the spheres imder central forces, that this chance must be of th«
form
yp (ipi, ip^ &c.)rfyi...rfp^
where ^ = Oi, 4>i = a^ &c., are obtained by the elimination of
t between the equations of motion of the r group under the fixed
centre and boundary forces and those between its component atoms,
because there is nothing in the conception of a molecule beyond
that of a system with a number of degrees of freedom, and under
internal forces ; and in this case, considering the generality of th«
assumption as to the external forces, it would be impossible to con-
ceive the existence of any general equation, independent of the time,
between the variables, except that of the conservation of energy, m
that the chance in question becomes
4,{E,)dq^...dp^
where E^ is above defined, and it remains to determine the form of f.
If we considered a second group of one or more molecules con-
taining 5 degrees of freedom (where s may or may not bo eoual to
r, but, like r, is much smaller than n), and defined by the coordinates
and momenta ?H-i---?r+^ ;'^-fl■■■Pr^-^. then the two groups togethec
contain r + s degrees of freedom aohnod by the variables gy..p^^
and since r + s is small comjiared with n, tlje chance of this group
having its variables between g^ and gi + dqi...p^,&udp^, + <ip^t
must bo
^{E^,)dg,...dp^
But this chance must be equal to the chanco of the r group beio^
fixed in the state q^, gi + dg^.-p^ P^ + ^^Prf multiplied by the chanoe
of the remaining s group being in the state 3h-i> Jr+i + c'jH-i—
Prf«» pT+t + ^Pr+v where tne r group are so fixed.
MOLECULE
615
Now to find tliis latter cliaace we obserye that it ia the chance of
the s group being in their required limits of position and motion,
when the internal forces between the r and » group become forces
between the » group and fixed centres.
If the total kinetic energy of the r group in their given state be
T„ and that of the r+s group be T^-w '•>» **'*1 kinetic energy of
the s group must b« T^, - T,.
: Also if the total potential energy of the r+s group under the
influence of all forces be xh-d t^"* ^ made up of—
(1) Xn tl'S potential energy of the r group to fixed centres, and of
its internal forces ;
(2) X* similarly taken for the s group ; and
(3) ,x> the potential energy of the r and s group forces.
'And when the r group is fixed the potential energy of the « group
is reduced to (2) and (3), or is XrH~Xr-
\ Therefore the chance of the » group having its variables within
the required limits when the r group is fixed must bo
Therefore
or <!> £,) rP (E^. -E,) = ^ {E^.
rhercfore ^ (a;) = « '"' = c'^ suppose.
And the chances of the r group having its variables between the
limits y, and Ji + dJi.-J'r and p^ + dp, must, in the state of per-
manent or stable motion, bo proportional to
e-''^rdq^,,,dp„
whieh was to be proved.
Supposing now that the aggregate of molecules under considera-
tion consists of a number of sets of similar molecules, the number
of molecules in one of these sets being N, where N is very large,
and suppose that each of these If molecules possesses a degrees of
freedom defined by the coordinates q^.-.q^ with the momenta
Pi...Pff and that its mass is m. Three of these coordinates may
be taken as the rectangular coordinates of its centre of mass, in
vhich case the corresponding momenta will be mu, mv, mw, where
fi, V, and w are the componept velocities of translation of that centre
cf mass. Then in this case, if qi---qa,Pt-P<! ^ ^^ remaining
coordinates and momenta of the molecule, the chance of the mole-
cule's variables being within the limits x and x + dx...Pf and
J.- + 4P{r ^"^ ^ proportional to
-»(X+/) , , , , . -l^(a»+r«-Hi«)
c dz dy dz dq,. . .api e s du dv dvi...{l),
-where T, the kinetic energy of the molecule, is equal to
'vhere / is a quadratic function of the p's, having as coefficients
Ifnown functions of the q's.
If we integrate the expression (I) for all possible values of x, y, s,
'^*---9ff Pi--'Fff ^® obtain an expression of the -form
Be s dudvda (II),
■where B ia independent of u, v, and to, and ^=u*+i^+v^. From
the form of (II) it follows, exactly as in the cases of the elastic spheres,
that the chances of all directions of the velocity of translation of a
molecule are equal, that the mean velocity and mean square velocity
of translation of each molecule are
VwA ^
Tespectively, and that the mean kinetic energy of translation is — ,
And the same for a molecule of any set.
Again, if T be the mean total kinetic energy of the molecule, then
T=
III-
-l>(X-tT) dx...d
.(III);
)&d if we evaluate this expression, paying attention to the form of
7 as a quadratic function of the ;'s mentioned above, we shall find
for (III) the expression ^.
It follows from this result that each additional degree of freedom
of the molecule increases the mean total kinetic energy of the mole-
cule by the quantity — , which is the mean kinetic energy of trans-
lation parallel to any one of the axes, and that the total kinetic
anergy is proportional to the number of such degrees of freedom.
/ If, again, we integrate the expression (I) for all values of the
monsenta, we obtain an expression of the form
Ce-^T- dx dy dz dqt...dq^ (IT),
Inhere x is the potential energy of the molecule due to fixed centre
and to interatomic forces in the position defined \>y x, y,z, q^-.q^.
The dimensions of the molecule are so small that we may regard
forces from each fixed centre on different parts of the molecule as
parallel and equal and functions of the distance of the centre o^
mass from that fi^ed centre, so that, if the part of x arising from
these fixed centre forces be called Xi, Xi will be a function of x, y, 2,
and of these variables only, the remaining part of x (arising from
interatomic forces), which may be called Xb wiU be a function of
the <r - 3 variables q^. . .q^^
If in (IT) we write Xi + Xj fof Xi ^^d then integrate for all values
of qt...qg we obtain an expression of the fbrm
Dc-'^^ dx dy dz (T),
where P is independent of x, y, z, and therefore p the density of
the if molecule matter in the neighbourhood of the point x, j/, z, is
mDe-''Xi.
From these results all the propositions proved above with reference
to the aggregate of elastic spheres or monatomic molecules, as to the
correspondence of the physical properties of such an aggregate with
those of gases as indicated by the gaseous laws, may be deduced
also for this aggregate of polyatomic molecules. So that if 2" bo
equal to -j, or the mean kinetic energy of agitation of any one of
the aggregate of moving molecules, if r be the volume occupied by
unit of mass, r the number of molecules in unit of volume, and )
the mass of each molecule, we have, exactly i
1, pv=
t the case referred
and
pv=
rT.
We also get the ordinary hydroatatical equations
±=fX, ^=pT, ^=pZ
dx '^ ' dy ' ' dz '^
from this expression for j) combined with the equatioa
p=mDe-''Xi,
remembering that
^=-mX, ^'=-7:ir. ^=-m^,.
dx ay dz
Tivhence tlie coincidence of the physical properties of this a^^regate of
polyatomic moving molecules with those of a gas, on the assump-
tion that the temperature represents the mean kinetic energy of
agitation, is at once apparent.
It can be shown also that the aggregate of moving molecules,
such as we conceive a gas to he, possesses another very important
physical property which, by its analogy to the second law of thermo-
dynamics, affords additional evidence of the relation between the
phenomena of heat and those of aggregates in some kind of motion, —
the property in question beiog that, if in any aggregate of moving
molecu^ the mean kinetic energy of any one of thfm be called
r, and if 5Q be an increment of energy imparted to the aggregate
from without, then -^ is a perfect differential.
If to this aggregate we apply a certain small quantify SQ of heat
or energy from without, and if <Jr be the increase of the mean
kinetic energy of agitation when the volume is unaltered, then
this constancy of volume prevents any of the energy SQ from being
absorbed in doing external work ; but it is conceivable that the
increase of t may cause such a change in the average state of the
molecule as to produce a variation 5x in the mean potential energy
of the molecule, dx being proportional to 5r.
Therefore
therefore
2A 3 2A 3 '
If the volume vary by Sv^ the pressure being constant, then we must
add external work, or p5v, to the energy absorbed , so that if the whole
external energy now applied be S'Q, and the increase of tempera-
ture St be the same in Doth cases, we have
r(^ + ^)ST+pSv
yO_ V 3 drj
But if ^ be constant, then as before
pjj,=2 ^ Jt,
616
and therefore tno ratio of i'Q to 5Q. or of the two specific heats
constant pressure ana cunstam volume, respectively, becomes
0 ( 3 ^ f 2
MOLECULE
r + 3
dx
- ' ^ is UBknown in aU respects erccpt that it must be positive ; also
vo know that <r must be integral and not less than 3 ; . if we denote
■* -^ by c we have for the ratio
<r + 2 + «
<r + e
1 +
' + e'
which, with the necessary limitations of o- and «, cannot be greater
than 1 5 or 1 -6, and in this limiting case the gas must be mon-
atomio.
If, therefore, any value above 1 -6 of the ratio for mercui-y vapour
be msisted upon, the theory must be abandoned so far as present
investigations are concerned. Il', however, the difference between
1-6 and any higher value given by the observations be regarded as
mtbm reasonable limits of experimental error, this value for mercury
vapour, a gas which on chemical grounds is regarded as monatonuc
may be viewed as confirming the theory, at least ;5to lanto.
If two sphencal atoms were united by a rigid rod to form a mole-
cule, such a molecule would have five degrees of freedom and the
specific heat ratio would in this case be IJ, for e would then "be
""T' ■, ,^ .,^ ^''^ ^ plausible approximation to the observed
value 1-408 of the ratio in a great number of two-atom gases, such
as hydrogen, nitrogen, o.xygen, and others, but all observations
agi-ee so completely m the ratio 1-408, or from 1-405 to 1-408 that
It hardly seems reasonable to regard the difference -008 as within
tlie limits of experimental error, unless, indeed, wo had grounds
tor suspecting a tendency to excess in all the methods employed for
the determinatioa of the ratio. But there are other difficulties
more formidable still, arisiug from the spectroscopic properties of
heated gases. The light emitted by such gases, so long as thev are
of no great density, never presents a continuous spectrum but a
y.ectrum consisting of bright lines mth intervening dark spaces.
thus the spectrum of hydrogen gives thirty-two bright lines that
ot mercury vapour sLx Unes, that of nitrogen eighteen, and so on
bo long as light IS regarded as an energy intercommunicable with
heat, and light of dehnite refrangibiUty is referred to vibrations of
given penod, -we must regard these discontinuous spectra as con-
nected with, asd arismg from, vibrations of determinate periods in
the molecule of the heated gas. And if a gas such as hydrogen or
nitrogen be constituted as we are supposing, of an indefinite repe-
tition of similar molecules it must follow that such molecules must
be capable, at any rate when not too closely packed together of as
many independent vibrations as there are bright lines in the spec-
trum ; that IS to say, m addition to the three degrees of freedom
arising from motion of tean^lation in solid space, each molecule
must possess as many additional degrees of freedom or possible
^^lij? The degrees of freedom corresponding to motion of
Shraton? ■"°"°.* r" ™°f-''»'te anything to these luminous
.T,v1?r\ T"/-*".^,^''^ .'"''''?'"' i"<=g"larity and independence of
f^Z tZ • f I "" otherwise with the internal or relative degrees of
J^n^V "° «™''' '^'•' ""^''^ *= S^' ^^ ^«T d™se, we may
^d C n.^r V"*"'°,' "»'«"?' °f ^0 between one encounter
?-„! T j^°y molecule with another for very many vibra-
ros^-i„r^f hT'^.S to its own law, to take place hi therektive
positions of different parts of the molecule. At each encounter the
ip".rlr'''" ''^'°'^'* be roughly shaken, and when the encounter
h, r^l r'^f,"? ""' "'"■ftions would become irregular and
d?fin?te r^.3^"V-l'^°8™<"^'" '"^ * g^"*"-^' diffused lifht of no
A-ul tM,^ ^ .I'^^V-'?* ^ ""=''' degenerates into mdinary noise.
A.id this is exactly what occurs in the spectra of dense gases.
To bring the theory, therefore, into agreement with observed
T....nomena, we renuire veiy many more degrees of freedom in each
u'.ecule than could possibly bo assigned to it in accordance wit
t.:<- observed value of the ratios of the specific heats, -mercury
V ., our, for example, admitting with difficulty the minimum number
ol three such degrees, as we have just now seen, while its spectrum
ju. Id require at least nine. And thodifficulty increases as we pass
to iiydrogon and other gases. '
.t,^ j-?'°'!LP",'"'P\'"'"'^°'^''' '^"' '"^ ^"^ of possibly explaining
th: difficulty that there were in all gases a number of cTmposTtf
iTf Mules fnth many degrees of freedom mixed up with the other
nr icules with three or five such degrees, but in so email a propor-
t.o to these molecules that thwr presence produces no appreciable
tu t upon the specific heats ; or, since wo have no experimental dc-
termnation of the specific heats of gases at light-giving temperature
we might at leasj untJ such expei-imental determination has beeii
arrived at, conceive that our atoms may change their constitution
under increased temperature, and become themselves capable of
vibration. There is nothing in the conception of an atom ai wo are
considering it which is really inconsistent with such an hypothesis
Certam obscn-ed phenomena accompanying dissociation andccin-
bination give nse to other difficillties in the way of the acceptan--
of the kinetic theory, in addition to those arising from the err 1 1
distnbution of mean kinetic energy just now discussed. For .1 -
mtrogen and hydrogen, for example, are mLxed in proportion tofo-ii
ammonia it is observed (1) that at ordinary temperatures thev'io
not exhibit the slightest tendency to combine directlv with ea-h
other, whUe on the other hand, (2) ammonia at ordinarytJmperatu- es
does not exhibit the slightest tendency to decompose into nitrog-ii
or fiydrogen. But ammonia when subjected to certain ven- hi<rh
fcmperatures becomes partially decomposed-that is, becomes" a
mixture of so many parts of ammonia and of so many other parts
ot nitrogen and hydrogen in the proportions to fbrm ammonia - and
U the temperature be high enough the decomposition may be 'com-
plete, but, in accordance with the kinetic theoiy, the conditions,
whatever they may be, which at high temperature cause the ammonia
to decompose, must sometimes occur to individual molecules at
ordinary temperature, because temperature, as we understand it
merely indicates a certain quantity ot kinetic energy, and therefore
in a gas, however cold, there will be always some molecules in a
state for dissociation ; and tbas dissociation having taken place can
by (1) nevei: be compensated by recombination ; tTierefore dissocia-
tion should be gomg on in ammonia at all temperatures, and thi3
result IS contrary to the observed phenomena (2). It might possiVi v
be conceived, as a way of meeting this last-mentioned difficulty, thJV
the dissociation attendant upon high temperature-that is, upon an
aver.^« large molecular velocity of translation-requires that thee
should be a fairly rapid repetition ot encounters among molecules
moving with dissociation velocity to ensure the production of dis-
sociation, and that in the case of a gas at low temperature, or small
average velocity, the chance of two molecules encountering one
another at^ high velocities is smaU, and the chance of any molecu'e
iS^pl^fi"" ?*? "T'^ succession of such encountei-s is piacticallv
insensible, and therefore that the dissociation spoken of reallv nevi
takes place. j "o-^i
As above stated, we conceive that in any gas at ordinary pressure
and temperature the mtermolecular forces are very small in the
aggre^te— that is, in Clausius's language, have a veiy small virial —
.t-y wmch is understood, not that tlie forces themselves wh'»r«
acting, are small, but that, considering the whole acgre'<^te "c^
molecules at any instant, there are very few pairs near enosgh lo
each other to exert any appreciable force on each other. Or if we
could watch any mdividual molecule for any time, we should find
that dunng by far the greater portion of the time it was sensiblv
Jiee from any action by surrounding molecules. The distanc,-
traversed by the type molecule between the instant when it passes
out of the sphere of action of one molecule and the instant when
It passes into the sphere of action of the next— that is, from ope
encounter to another— is called its /ra^rt^A.
We may find the chance that a molecule starting from any point
with velocity <j in a uniform gas shall have free path between x
and X + dx from that point.
^f "^ be the chance for such a molecule of free path al least unity,
then a? is the chance of a free path at least 2. Hence the chance
ot tree path at least x must be of the form a'.
Following the method employed by 0. E. Jlever,' let us write
this in the form
where therefore i
log a *
then the chance of free path .i; -Kir is
e I .
The chance that such a- molecule shall have its first encounter
between s and a+dx is the difference of these two expressions-
tliat is, X "^ '
I'
This is the chance of a free path beti\-een a: and x+dx.
The mean free path for such a molecule must then b« ■
i t' l^dx-^( c''Ldx=l.
Jo ' J a I
This is the meanmg of the const.int line I . But if we denote
by 3 the' nutaber of encounters which a molecule moving through
space with velocity u exi>criences on the average per unit of time, i
* KijuliKht Thnrit der CoK, Bnalau, ISTT.
MOLECULE
617
B=^; or .
Hence the chance for such a molecule of free path between x
s.ndx+dxia
— e ^ ax,
with the above definition of B.
The chance of a molecule whose velocity is u havin» free path
X is of course the same as the chance of its free path having the
duration — . If * = — , the chance of duration behveen t and t-^-dt
is thnb B ».
— »-'" udt ; or Se'^ dt.
a -
Meyer detmninSs the value of JB, if the molecules be spheres, in
the form
B = AVs=n i 1 + ■
(-)"■
fir 2re - 1 ■ 2^^ + 1
(^V:)'
..},
where JJ = — t= , and s is the sum of the radii of two molecules
it will be observed that the series converges very rapidly if oi-A
'j less than unity, the successive coefficients being
210 ' 1512
11880'
,8sc.
Having found B for the number of encounters experienced per unit
of time by a molecule having velocity u, we have for the average
number of encounters experienced by any molecule per unit of time,
which we denote by C,
°=:j7^^1 «-*"'"'£.?=..
From which Meyer deduces
h
Hence the mean value of the free path foi all mc^eouleSj irrespec-
tive of velocity, is X= — - = = — •„ .
Thns the Icinetic theory of gases presents to us the conception ef
apparently perfect rest, as the result of motion irregular in detail
but permanent and stable on the average. Whatever difficulty
luay be felt at first sight in the acceptance of this theory in the
casj of a medium at rest is greatly enhanced ■when we pass to the
Cdiitemplation of a disturbed medium like a mass of gas through
which a wave of sound is passing. In our. ordinary iuvestigations
of cuch a disturbance the gas is treated as a continuous body, sub-
jected to small relative motions of its parts, accompanied by corre-
sponding variations of internal pressure. "WTien a disturbance or a
local condensation or rarefactiou is set up in any portion of this gas
■ft-e calculate the resulting effects by the well-known equations of
sound motion. But on this kinetic theory the medium is supposed
to consist of a number of discrete masses — elastic spheres or the
like — which preserve the physical properties of the medium merely
by the recurrence of their mutual collisions, such collisions obeying
no law in individual cases, but preserving a certain average uni-
formity in the motion of the whole aggregate ; and we need some-
further investigation to assure ourselves of the applicability of the
ordinary ti-eatment of wave motion to such a medium.
Kow we observe that the physical properties of -our medium, so
far as the relation between pressure, density, and temperature is
concerned, merely require that the temperature be measured by the
n:ean total kinetic energy of ti-anslation, and that the mean kinetic
energy of ti-anslation parallel to any fixed line be equal to oue-third
of the mean total energy of ti-anslation. If the molecules constitut-
ing any portion of this medium were animated by a common velocity
or acceleration, the physical properties of this portion would be
similarly determined by the velocities and kinetic energies relative
to the common motion. "When the distribution of such relative velo-
cities is stable or permanent, the average relative kinetic energy in
any fixed direction is one-third of the average relative total kuietic
•"eBCTgy, such property constituting normal distribution.
Suppose that in any portion of a medium, consisting of equal
elastic spheres, this distribution has been disturbed — that is,
Xvivr, 277iv^, and 'Zmv^ are unequal.' If Fwere the relative velo-
'ci^of any paii- of spheres after such di^tuibance and before they
cofiide, and Q the angle between V and the common normal at the
^int of impact, then the normal and tangential relatiyejtelocitifis^
before impact are Fcos 0 and Tsin 0, anoLafter impact they become
- Kco3 e and Ksin $ respectively. Tlic relative velocity after im-
pact, resolvefi in the direction of relative velocity before impact, ia
therefore ^ -
- Tcos-fl+rsin^fr,
or - F'cos2^ • and the chance of 0 being between 9 and 0 -^016 la
fiin 10 do,
•Hierefore the average square relative velocity resolved in the
original direction becomes after impact
Vi
Ir'
28 sm 20 1:9. 01 ~.
The relative velocity after impact ia the plane of V, and the
normal perpendicular to the direction of V before impact is
r siad cos e+r sine cos ff, or r sin 29.
And, if a fixed line be taken in the plane perpendicular to V, the
average value of the square of the relative velocity after impact,
resolved pai-allel to this line, is
V
■a
1/3
sin' 29 cos'^ d9 d<j>, or -j- as before.
Hence we conclude Jliat, in whatever manner the distribution ia
disturbed in any portion of the medium at any instant, it will, for
all those pairs of spheres which within any given interval encounter
each other, have assumed the normal distribution after that inter»-al.
If T denote the average time between two collisions for any given
sphere, the chance that this sphere shall continue for any time t
_ t_
free from collisions is, as wo have seen, e t .
If, therefore, D be the number of spheres within any region whose
total relative velocity is between w and w + <iw, but so distributed
that the mean square of their relative velocities along any fixed
line is not — -, then after a time t considerably greater than r, say
ten times t, the number of the D spheres which have escaped col-
lision will be utterly inconsiderable, and the distribution will have
become normal througliout the region.
Suppose, for instance, that a sound wave is passing along a tube
filled with air.
(E
D
the air in the tube is, -at any instant, in a state of alternate com-
pression and rarefaction, as at C, E, C, R above.
If the note sounded bo (say) 500 ribrations per second, the length
of the wave CR is about VjV feet, and the time taken by the wave
in traversing that distance is about j^jth of a second.
The air in any section of the tube near P has alternately a small
positive momentum and an equal smaU negative momentum, the
reversal taldng place in everj- rrjth of a second ; also the same cause
which produces the average momentum in either case disturbs the
distribution of energy among the x, y, and 2 directions, i.e., it is
always producing an excess or defect in mu- above or below that of
rmfi and mM.-^. By what has been proved above, this abnormal
distribution of energy becomes inappreciable, owing to molecular
collisions in a time considerably less than nj'inith of a second — in
fact, in about TsirsinniTith of a second, when the value of T for
atmospheric air is considered. It is therefore legitimate, in calcu-
lating the velocity of sound in air (at least on the elastic sphere
hypothesis), to regard the distribution as always normal in any
section of the tube, the air in that section or in any elementary
portion of it possessing, as a whole, any given velocity or accelera-
tion, estimated as if we were dealing with a continuous mass.
Diffusion op Gases.
If any further light is to be thrown on the physical
nature of a molecule from investigations, experimental or
analytical, concerning gases, it wUl most probably be b'y
means of experiments on the diffusion of gases, or else on
the internal friction or viscosity of gases, and the com-
parison of these results ■with those obtained analytically
by the methods of the kinetic theory. Such investiga-
tions have been undertaken experimentally by Graham,
Loschmidt, Maxwell, O. E. Meyer, and o.iiers. An ac-
count of them will be found in O. E. Meyer's work above
referred to. The same problems have also been discusses
analytically by Maxwell,' and by Stefan, O. E. Meyer, anc
Boltzmann in the treatises referred to below. We pro-
ceed to give a short account of ileyer's results.
^-JShiL.Mag., July 1860, and Feb. and M.ttcU 1863.
XVI. -^ 73
618
MOLECULE
;The term " diffusion " has sometimes been applied to the
process by which a gas passes through a porous diaphragm.
This, however, is now generally denominated transpiration.
It has also been applied to the expansion of a gas into
Tacuum, as on the removal of a diaphragm separating the
gas from an exhausted receiver. This is now generally
denominated free e.xpansion. We shall understand, as is
now usual, by the term diffusion the process by which,
■when two or more gases are mixed throughoui. any space
in different proportions at different points, but so that if
all molecules were of the same gas the whole would be in
equilibrium, the different gases pass through each other
and tend to equalize the proportions at all points in the
space.
Suppose, for instance, a tube containing a mixture of two gases, A
r.nd B^ at constant temperature and constant pressure of the com-
bined gases throughout the tube and subject to no forces, but tho
density of gas'^ increasing and that of B diminishing from one
end of the tube to the other. Let the axis of the tube be taken for
the axis of x. If N^, be the number of molecules of gas A, and iVj
the number of molecules of gas B in unit volume, we have, owing
to the constant pressure and temperature at all points of the tube,
jS'^-\- Nf,= Ny a constant. But at a given instant N^ andiV^ at any
point are severally functions of x. It will be found that under
tliese circumstances more molecules of gas A pass through any sec-
tion of the tube, which may be in the plane of yz, in one direction,
i^?.y from left to right, than in the opposite direction. On the
rther hand, more molecules of gas B pass from right to left than
from left to right. And this ■will go on till the mixture becomes
uniform throughout the tube.
The investigation of the rate at which the unequal distribution
tends to equalise itself in this simple case— that is, the excess of the
number of molecules of gas A which cross a section of the tube from
kft to right over the number crossing in the same time from riglit
to left — is the problem of diffusion. We give the results obtained by
O. E. Meyer as follows: — if the molecules of the two gases had the
same mass and dimensions (t» put an ideal case), then the excess of
molecules of either gas passing through the section in one direction —
that is, the stream velocity — would be-g -3-^ wi, where I denotes
tho mean free path for a molecule having velocity w, and wl is tlie
average value of that function for all molecules of the gas,
' When we come to deal with two gases, the molecules of one not
being of the same size and dimensions with those of the other, we
ehall find that, in the absence of any common velocity of the two
biases at the plane of yz, more, or fever, molecules of gas A would
cross the plane per unit of time from left to right than of gas B
from right to left, because, assuming constant pressure and tem-
jierature of the mixture at every point in the tube, the number of
molecules of the two gases combined must be the same at every
|r>oin*'--*'bat is, iV +iVj = JV, where A' is constant. Heuco
dN'„ dN.
dx
dx
^Now the excess of molecules of gas A coming from left to right
per unit of time is
1_ dN^
3 dx
iilat and similarly the excess of mole-
cules of gas B crossing from right to left per unit of time is
-^ r-j— * w/j,, if we now distinguish by suffixes a and b quantities
relating to the two gases respectively. Here 7^ and 7^ are mean
free paths for velocity w of the two kinds of molecules through the
mixed gases, and w^^ ^ ^^^ generally equal to uly Hence the
total number of molecules crossing the plane from left to right ex-
ceeds the number coming from right to left by -g- jZ i^^a ~ ^^h)-
r Meyer here assumes that the combined gases have a common
velocity '- -3- -^ (w^a - w^t), and that such common velocity
will not affect the relative motion of tho molecules. On that hypo-
thesis the rate 0 1 diffusion can be calculated as follows. The pro-
portion of the Bt earn of tho combined gases which consists of mole-
cules of gas A i»
^, 1 dN, ,_ ' _ .s
..'W^N, S dx Wo -"'»', •
Hence tho total surplus number of molecules of gis A passing
tlirough unit area of tUo piano per unit of time is/
The expression
B^f-1'V^^H-.V..-U
3A^
[N-j,ul^ + N^ulf}
is defined to be the " coefficient of difiiision " of gas :a^inlo^(a$ B.
It is evidently the same as that of gas B into gas A,
2'he Jiclation of the Coefficient of Zfijiusion to Density. — 1: can
be shown that l^^, the mean free path for a molecule having v<:\o~
city w, is for any single gas inversely proportional to the density^
and for any mixture of gases inversely proportional to \ the ag-
gregate volume occupied by matter in unit space. 'HeUce^ in thd
expression -^ wl -j-, cjI is inversely proportional to fKe density,
or to X, as the case may be.
' Now the lite of diffusion on this theory depends updlT- * "^
3 dx
per unit of
Hence, given the absolute increase of density of a |
length, that is, given -j—, the rate of diffusion ought to vary in-
versely as the density of the combined gases. On the other hand,
given the proportional increase of the density, or -^ -3^-, the rati of
J^ dx*
diSusion ought to be independent of the density, because in that ■:aiie
dN — ■ ' ■
J— varies directly, and ul inversely, as N. The analytical result,
djy
that at given temperatures, and given the absolute value of ^— , tha
rate of diffusion is inversely proportional to the density of the gases
agrees with the experimental results obtained by Loschmidt for
carbonic acid gas and air, carbonic acid gas and hydrogen, hj'drogea
and oxygen.^ . ^
Jiclation of tTi^ toefficient <if Dijfusian to Tanpcratit're. —Tho^
coefficient of diffusion varies dii-ectly as the square root of the al. >o-^
lute tcn'.perature, for
VA
•^l=ir.
'2;i(j--f-i I
'-Wir.1
line'
f=\;a
or, if u\^=fj
vX
£ VTrJ^V
where ^ denotes a certain function, and
(I) - '■^/>--^"7J
This analjiiical result also agre
ments above refeiTed to.
fairly with Loschmidt's oxji-'a-
Fkiction ok Viscositv of Gases.
Suppose two layers of gas separated hy an imaginary
plane, similar in all respects except that the molecules of
one have a small common momentum in a certain direction
parallel to the plane.- We may take the imaginary plane
for that of y:, and the average direction of motion of the
molecules on one side of the plane, €.17., the left-hand side,
for tho axis of y, the molecules on the right-hand side ol
the jilane having no average momentum. Then tho mole
cules crossing from the left to the right side carry witl
them an average momentum in the direction y, and so tenc
to impress the right-hand .«tratnm of gas with that mo
mentum.' On the other hand, the molecules of the right
hand stratum crossing tho plane into the left-hand on<
have, relatively to the molecules in the latter, an average
momentum in the opposite direction, and therefbre lend U
diminish the average momentum of the left-hand stratum
1 SUiunaitierichtc, 18V0, Dd. 1x1. 8. 880. • "• See Mcvcr'8 Kin. Thcorit, p. ^.'
MOLECULE
619
ISence, if we attempt to cause one stratum of gas to pass
over another in parallel planes, we experience ■» resistance
due to the intercliange of molecules between the portions
•f gas separated by the plane. This is in some respects
analogous to sliding friction between solid bodies, and is
called by German writers the " friction " {Reibung), by Max-
well and others the " viscosity," of the gas. Meyer ^ investi-
gates this effect of friction in a manner somewhat similar
to that employed in case of di6Fusion, and obtains for the
coefficient of viscosity J mNid.
Relation of Ou Coefficient of Vixosity to Density and Tempera-
ture.— The viscosity of a gas is independent of the density, being,
according to 0. E. Meyer, —^ ul. Now, for any one gas, l^ is, as
we have seen, inversely proportional to the density, and therefore
(di is inversely pnjportional to the density. On the other hand, N
is directly proportional to the density. Hence the viscosity is in-
dependent of the density. This agrees with the result obtained
by Maxwell from the kinetic theory in 1860, and with the results
©f experiments by Maxwell^ and O. E. Mey>;r.* Also, experiments
by O. E. Meyer and Springmiihl * on the transpiration of gases show
that the times in which two dijferent gases under similar circum-
stances flow through a tube maintain the same constant ratio to
one another. As in the case of the coefficient of diffusion, wl is
inversely proportional to the square root of the absolute temperature.
As both the coefficient of diffusion and that of viscosity depend
on the same function ul, it should be possible from experiments on
viscosity to determine the rate of diffusion. E.xperiments with this
•bject have been conducted by Stefan* with very satisfactory "results,
his calculated values for the coefficient of diffusion agreeiug very
closely with those determined by Loschmidt's direct experiment.*
■ We have given the above results for the coefficients of diffusion
ind viscosity from 0. E. Meyer's work, because his method has met
with very general acceptance. It has been shown, however, by
Boltzmann,' that the method is incomplete. Meyer's results can
only bo obtained on the assumption that the molecules of a gas
undergoing diffusion or internal friction, which have any given velo-
city, as«j, are moving with that velocity in all directions indifferently.
We may calculate the number of molecules having velocity to that
pass through a given plane during a short time di, starting from
encounters at any given distance from the plane. If we assume
that the molecules, issuing from such encounters with velocity tr,
move indifferently in all directions, we obtain Meyer's result.
This assumption is true only of a gas at rest — that is, having no
velocity of translation — so that our result so obtained would express,
ia case of diffusion, the rate at which two gases be<Fin to diffuse, if
given at any instant both at rest — that is, with no stream velocity
— but mix^ in unequal proportions in different parts of space.
In any actual case ol diffusion, either of the two diffusing gases
fir: quires a small velocity of translation. If we take this velocity
into account in calculating the number of molecules of the gas
passing through a plane, according to Meyer's method, we shall
find that it introduces two new terms, one of which, when the
motion becomes steady, is equal and opposite to the result obtained
by Meyer. This is proved by Boltzmann in thp case of viscosity in
i.ie treatisa above referred to. The same proof is easily applied in
the case of diffusion.
Stefan's Method. — Stefan * regards the two diffusing gases as
Laving small velocities of translation, or stream velocities, itj and
lip in opposite directions, so that the molecules of one gas, of
mass mi, nave an average momentum wtjW, in direction from left
to right, and those of the other gas, of mass m^ an average mo-
mentum TTi^Mj from right to left By virtue of encounters between
t'ae two sets of molecules, each gas is always imparting to the
cJier a portion of its own average momentum, and receiving
fiom the other a corresponding momentum in the opposite direc-
fon. The momentum so transferred or interchanged is what
S tefan calls the rcsistaiiee which one gas offers to the other's diffusion.
In this investigation Stefan assumes that all classes of molecules
of one gas, whatever their molecular velocity in space, have the
f 'jne average velocity in the direction of diffusion — that is, the same
s ream velocity — so that the motion of the molecules of a diffusing
gas would be exactly represented by considering the molecules of a
gia at rest — that is, with only its molecular velocity — at the same
« PoggenaorJ^f AnnaUn, 1871, cxliii. 14.
• Pogg. Ann., 1873, cxlviii. 1 and 526.
• SiUttn^ii)fT. d. k..k. Akad., 1872, Ixv. 323.
• For a foil account of these aDd other expenmesta on dtffbsion and vis-
jlty, sec O. E. Meyer, Sinctiaclu TKeorie d. Coat, mder the heads " Reihong "
d "DiffQsion."
? " Zor Oas-BeibODg," in the Silinnfthtr. d. t.-t. Akad., 1881.
;• Hemoir " On th" Dj-camical Theory of Diffusion" (oitainjjier. d. *.-t Aiad.,
temperature and pressure, and then giving to each molecule the"
additional common velocity u in the direction of diffusion. Bolti-'
niann, however, shows that, in order correctly to represent the motion'
of the diBiismg gas, we must impart to molecules having different
molecular velocities independent of direction different c-ramon
velocities in the direction of diffusion. And it will be found that
the resistance of the gases is sensibly modified by this property.* j
The complete solution of the problem,— that is, the determina^
tion of u as a function of to, on the hypothesis that the molecules
are elastic spheres, — is difficult.
If we assume molecules to bo centres of force varying inversely as
the nth power of the distance, so that the force at distance r is --,
where ;i is constant, we obtain the following result We assume
the molecules of gas .4 whose absolute velocities are between
v> and w + dwto have an average stream velocity « in direction of
the tube, where u is a function of w. Then, if the terminal con-
dition at the ends of the tube be maintained constant, we obtiin an
equation of the form
p dX'^_in-8„ m,m, rN^N^
N dx Zn-Z ' Bij + 171, unit volume
multiplied by the average value for all molecules of gas A of
u F'''~',whereristherelativevelocity of two molecules, one taken
from each j,as, and C is a constant, and ot„ m, the masses of the
molecules cf gas .<^ and gas B respectively.
By making n infinite we obtain the result for elastic spheres : in
»-5 ''
that case r''-l = r, and the problem is to find the average value
of uV.
Since p varies as the absolute temperature, and the average valuo
of T varies as the square root of the absolute temperature, we mav
infer that the average value of u — that is, the stream velocity — will
vary approximately as the square root of the temperature, as it
appears to do from experimental evidence. If, on the other hand,
n = 5, V disappears, and _3 = ^- 1° this case the analytical de-
termination of u presents no difficulty ; but in the result the stream
velocity varies as the absolute temperature, which accords less satis-
factorily with experiments.
On MoLECtTLAR DIMENSIONS.
Many attempts have been made in recent years to form
an estimate or conjecture, more or less accurate, of the
numerical value of the dimensions of a molecule and the
absolute force between molecules.'"
In accordance with the view of the subject consiucred
in this article, we are here concerned with such specula-
tions only in so far as they are founded upon the kbietic
theory of gases, or supported by it. The phenomena of
diffusion and viscosity especially have afforded grounds for
estimates of molecular dimensions.
It is first necessary to define what is meant by the
dimensions of a molecule. Regarded as an clastic sphere,
it has dimensions with the conception of which we are
familiar. It is not, of course, seriously contended by any
physicists that the molecules of a gas are actually hard
elastic spheres, exerting no force on each other at any dis-
tance greater than that of actual contact, and then an
infinite force. It is necessary to conceive the forces as.
finite, although they may diminish so rapidly with the dis-
tance as that the motions of molecules in the aggregate
differ little from what they would be if the molecules were
ideal elastic spheres. Nevertheless, they must be finite
forces ; and, that being the case, it is diffiqult, if not im-
possible, to frame a definition of the boundary of a mole-
cule, except as a certain surface at which the forces acting
between the molecule in question and other molecules
attain a certain value.
If, for instance, we were to regard a molecuie as a centre of force.
* For Boltzmann's own treatment of the subject we cannot, within the limits
of this article, do moro than refer the reader to the memoir above mentioned,
" Zur 6as-Beibung." and another as yet nndnlshed memoir " On Diffusion," in
the Sitsufi^sbtr. d. k..k, Akad., 18S2. - |
w An account of these wiU be found in O. E. Meyer's Kin. Tkeorit d. Case,
in Professor Tail's Recent Advanced in Physical Science, lecL xii., and in the
foUowing memoirs :— /"Ail. Jfo?., July 1879, " On the Size of Molecules." by N.
D. C. Hodges; Phil. Mag., March 1830, " On the Mean Free Path of Molecule^"
by the same author. See also, lecture delivered by Sir \i. Thomson at the.
Royal Institution, 2d Feb. ISS3.
620
MOLECULE
iexcrting an attractive force -^ and a repulsive forco -rf, we iniglit
define the molecclo to ba a sphere of radiua a, sucli that -4=— 7.
In like manner, regarding a molecule as a centre of force, repelling
Rccordirg to the law of the inverse fifth power of the distance, we
might define the magnitude of a molecule aa a sphere of radins
equal to the least diatence to which two molecules, whose relative
velocity is equal to the mean velocity of the centres of force,
approach each other In a direct encounter.
If Oil any hypothes^ concerning the nature of a molecule, or the
law of force which acts during encounters, we caa calculate the co-
efficient of viscosity or diffusion anal}iicaUy, a compariBon of the
auaiytical result with results obtained by eyjwrimeafc may afford
the means of determining the absolute numerical value of the con-
stants used in the analysis. For example, if we consider the mole-
cules as clastic spheres, and if we consider for a monlent Meyer's
results as correct, or approximately correct, the coeflBcient of
viscosity for any single gas can be put in the form. -5- wZ^,
v/here N is the number of molecules in unit of volume, m the mass
of a molecule. Now, for every value of w?(j, the mean free path
of a molecule with that velocity is equal to \/h ^ -3, where s is
tivics the radius of a molecule multiplied by a numerical factor
which can he determined to any required degree of accuracy. Also
at given temperature and pressure the numerical value of \//t is
known. It follows that we can calculate the numerical value of
the ceelScieat of viscosity by analytical methods in terms of A^irs^
to any required degree of accuracy. Let it be jy^ • If by experi-
ments on viscosity we can determine the numerical value of the
same coeflScieut in the form C^, when C\ is a mere numerical quan-
tity, we have immediately the equation C^— -^—i, or Nirs^ = -^ ,
This pives in absolute numerical measure the value of Ntr^, or
four tunes the sum of the great cii'cle areas of all the molecules in
unit of volume, supposing them to be spherical. If we attempt to
use the coefficient of diffusion instead of viscosity in this method, we
are met by the difficulty that the azialytical result contains now
two unknown quantities Instead of one — namely, the radii of the
respective molecules of the two gases in quesrion. If this difficulty
be got over by a comparison of results obtained in different ex-
periments, the greater ceitainty attending the observations on dif-
fusion might perhaps compensate for the additional mathematical
difficnlty, and render diffusion at least equally trustworthy with
viscosity as a method for estimating molecular dimeneions. Again,
on the hypothesis of repulsion between molecules according to the
law of the inverse fifth power of the distance, we can calculate
analytically the rate of diffiision betweeu two reservoirs connected
by a tube as above described, the result containing only one
\inknown constant, viz., (i, the constant of absolute force. Com-
Saring the analytical result with the results of experiments on
iffusicn through such a tube as above described, if we find them
capable of being harmonized by attributing any numerical value to
(i^ wo should have good reason for concluding that the law of force
assumed is to a certain extent at least the true law, and that the
particular value of /i is that which harmonizes the analytical with
the experimental results. And the determination of /:*, the absolute
force, conesponds to, or indeed is, the dotenuination of the size of
the molecule.
Until all the mathematical hypotheses have been fully developed,
no very great reliance can be placed on the results of such com-
parisons, even assuming that the experimentsd results themselves
are to be depended upon.. However valuable the experiments may
be for other purposes, they are not valuable for the purpose of
dctei-mimng molecular dimensions until our mathematical analysis
is sufficiency advanced to enable ua to interpret the experiment.
At present it is perhaps impossible to deduce from the experiments
any other result bearing on this quesrion than that the coefficients
of diffusion and viscosity increase with increasing temperature, and
probably contain an important term proportional to the square root
of the absolute temperature. If, indeed, it can be ehown that that
is the only term, and tf it can be also shown that the density of one
of two diffusing gases in a tube through which steady diffusion is
going on tends to vary in geometrical progression, then the analysis
will lead us to the conclusion that molecules of gases behave in
their physical relations to each other as if they were elastic spheres.
The following method has also been suggested for estimating the
magnitude of molecules of mercury. Mercury is regarded by most
chemists as monatomic. Let us assume that its molecules are con-
ducting spheres; on that assumption wo may calculate the specific
inductive capacity of mercury vapour on Faraday's hypothesis to be
\_\t whore X is the ratio which the aggregate volume of all the
spherical molecules in unit volume bears to unit volume. If now
K, the specific inductive capacity of merciry vapour, can be deier-
mined experimentally, the equation K= -z — r affords a ground
for estimating the value of X, — that is, the aggregate volume of the
molecules.
Another method, originally proposed by Van der "Waals, is founded
on the small deviations from Boyle'a law observed in all gases.
Suppose a vessel of volume V containing a. number N^ of Mastic
spheres, each of mass m, moving with a certain average kinetic
energy. Lot 77, be the pressure. Let a second class of elastio
spheres, in number N^, each of the same mass m as the former class
and having the same average kineric energy, be introduced into the
vesseL If the second class of spheres could freely penetrate the
first, and vice versa, so' that there should be no restTictions on a
sphere of the first class and a sphere of the eecond being in the
same place at the same time, then the pressure on the walls of the
vessel would be increased in the exact proportion
A'l
Boyle'a
law would be exactly fulfilled. But if the spheres cannot pene-
trate each other, the volume occupied by the seci/nd class of sphferes
is not Vy but V- ~^ A^jirr^, if r be the radius of a sphere of the
first class. Consequently, the pressure due to the second class of
spheres is rather greater than it should be, and there is a email
deviation from Boyle's law. Yan der Waals treats the pressure aa
proportional to the number of encounters, and therefore inversely
proportioaal to the mean free path, which is evidently diminish^
by any increase in the magnitude of the spheres, and diminished
more than in proportion by any increase iu the number.
(H. W. W.— S. H. B.)
Chemical Aspect.
Tlie word Molecule is used by chemists to express the unit
of a pure substance, that quantity of it which its formula
ought to represent. What this quantity is, in any particular
case, must be ascertained by studying the chemical actions
by which the substance is produced and the chemical changes
which it undergoes. We may give one or two illustrations
to show how this can be done, as well as to indicate the
limits within which these methods can be appUed.
The formula usually assigned to acetic acid is CoH^Oy
This agrees with almost all the chemical actions in which
it takes part. Thiis, one quarter of the hydrogen is
replaceable by other metals, as in CgHgKOg, &c. ; and one,
two, or three quarters of the hydrogen can be replaced by
chlorine. There must, therefore, be foui- (or a multiple of
four) atoms of hydrogen in the molecule. Similarly, half
of the oxygen can bo replaced by sulphur, and one-half of
the ozygen along with one-quarter of the hydrogen can
be replaced by chlorine. There must, therefore, be two
(or a multiple of two) atoms of oxygen in the molecule.
Again, the formation of marsh gas and carbonate of soda,
when acetate of soda is heated with caustic soda, and tb^
formation of aceto-nitrile from cyanide of potassium and
iodide of methyl, show that the carbon in acetic acid is
divisible by two, or that the molecule contains two (or a
multiple of two) atoms of carbon. CMfio is the simplest
formula which fulfils these conditions, but the existence of
an acid acetate of potash and an acid acetate of ammonia,
the fonnulse of which ^e usually written CgHgKOg,
C0H4O2 and CoH3(NH4)02, C2H4O2, as if these were com-
pounds derived from two mofecules of acetic acid, might
lead us to C4H3O4, as this shows that the hydrogen is
divisible by eight. In the same way, we can easily saUsfy^
ourselves that C^HioO^, or soin^ multiple of it, is the
formula of starch ; that CgH^NO, or some vudtiple of it, ls
the formula of indigo blue, and so on. But it is not easy
to determine by purely chemical methods whether thesf^
formulae themselves, or multiples of them, really represent
the molecule. A simple formida may suffice for a great
many of the reactions of a substance, and may enable m.
to represent a great many of its derivatives, . and yet
reactions and derivatives may be discovered which requira
a multiple of that simplo formula. This has already been
indicated in reference to acetic acid, and a. very striking
MOLECULE
621
illustration is supplied by meUitic acid. For a long
time the formula C,H20j Tvas used for this acid, and by
means of it all the then known derivatives were repre-
sented. But later investigations by Baeyer proved that
this formula must ba multiplied by three, the new deriva-
tives obtained by him not being capable of representation
with any formula simpler than CijHgOj^. Very many ex-
amples of the same kind might be adduced, but those given
may serve to show the nature of the difficulty of settling
the formula and with it the molecular weight of a sub-
atanoe. It need scarcely be said that the multiple formula
represents everything which the simple formula represents
and something more, and that chemists as a rule take the
simplest formula which will answer the purpose. These
chemical methods of determining the formula and mole-
cular weight apply equally to all pure substances, but they
do not give us absolute values, only numbers to which
tho molecular weights are proportionaL And for purely
chemical purposes these are all that we require. Thus,
■when a chemist speaks of acting on a molecule of suc-
cinic acid vrith two molecules of pentachloride of phos-
phorus, he means that he mixes them in the proportion
of 118 parts of the former to 2 x 177'5 of the latter.
For the sake of precision we sometimes speak of a mole-
cule of water (or other substance) in grammes, or even of
AgrammeJtnolecvle, AffraiTtr-molectile, &c. Thus, in the case
just mentioned a gramme-molecule of succinic acid means
118 grammes of succinic acid, &c.
But, while for practical purposes these proportional
niimbers are quite sufScient, we cannot leave out of view
their relation to the actual constitution of matter. There
is good reason to believe that matter consists of discrete
particles, and that every pure substance is made up of
small portions of matter, all alike, so that one of them, if
we could examine it, would give us a complete idea of
the chemical composition, constitution, and character of
the substance. These small portions, of which the smallest
quantity of the substance which we can examine contains
many millions, we may call molecules. From the character
which we have supposed this molecule to possess — viz., that
it fully represents all the chemical properties of the sub-
stance— it will be seen that these real, ultimate molecules
must be proportional to the molecular weights ascertained
by chemical means ; so that, while for practical laboratory
or manufacturing purposes we use the gramme, the pound,
or the ton as our unit, and speak of 18 grammes, pounds,
or tons, as the case may be, of water, as a molecule (or
gramme-molecule, ton-molecule, &c.), in dealing with the
actual constitution of matter we should iise as our unit
the mass of a single atom of hydrogen, and our gramme-
molscule would then be a definite, very large, but not yet
Mcurately ascertained, number of real molecules.
It has been already shown above that, on the kinetic
theory of gas, a gas consists of a number of particles
moving about in straight lines in all directions, and that
in a homogeneous gas which follows Boyle's and Charles's
l&ws these particles are all alike. The masses of the
particles of different gases are therefore to one another in
the same proportion as the densities of the gases, tempera^
ture and pressure being the same. Thus, in gases, the in-
dependently moving particles of the kinetic theory are the
molecules of which the chemist is La search, and it becomes
important that we should compare our chemically found
molecular weights with the densities. Theoretically accu-
rate results could be obtained only in the case of a perfect
gas ; but small deviations from Boyle's and Charles's laws
do not interfere with the application of this method.
Chemical methods, as we have already seen, lead us to a
particular number, or a multiple of it, so that our choice is
aa a rule limited to two or three numbers widely differing
from one another. We find that if we do not exceed the
limits of chemical stability a gas approaches the state of a
perfect gas 0,3 the tercporature increases, or as the pres-
sure diminishes. Now if one of the ntimters rendered
probable by chemical evidence nearly coincides vrith that
given by comparison of gas densities, under conditions
where the substance sensibly deviates from Boyle's and
Charles's laws, we find that by diminishing the pressure or
increasing tho temperature within the limits of chemical
stability, and thus bringing the substance nearer the state
of a perfect gas, the correspondence between these two
numbers becomes closer. This has already been pointed
out and illustrated in the article Chemistey, toL v. p. 469.
We can now compare the results, in the case of gases,
of the chemical and of the physical determination of
molecular weight, by giving some examples, placing side
by side the formula and molecular weight adopted by
chemists, and the mass, in grammes, of the gas occupying
the volume of 22-33 x 760/^? x (273 + <)/273 Utres. This
volume is that which one giamme of an ideal gas having
the molecular weight 1, and perfectly following Boyle's
and Charles's laws, would occupy at pressure p millimetres
of mercury and temperature t" C. If, then, w be the mole-
cular weight of any gas, w grammes of it should occupy
this volume, and slight deviation from this would indicate
slight deviation from Boyle's and Charles's laws. In vha
aimexed table w is the molecular weight and m the nuiss
contained in 2233 x760//>x (273 + i!)/273 litres. ViTiere
the temperature is not specially stated, the determinations
were made under the usual atmospheric conditions.
Sulphuretted hydrogea
Nitrous oxide
Ammonia „
Carbonic acid
Mavsh gaa
Olefiant.gas
Hydrogen ...
Oxygen
Chlorine ...
Phosphoms
Arsenic
Sulphur
Bromide of altuniiiium
Ferric chloride
oal-ammoniac
Oil of vitriol.,
Pentachloride of phos-
phorus
Sulphide of ammonium .
H,S
N,"0
co/
CH4
C,H.
I
Aljfer,
Fe.C!,
NH,a
HjSOi
PCI5
(NH,)^
71
124
300
102
34 04
44-08
17 12
44-14
16-13
28-44
71-27
125-9
294-6
194
63-5
537-5
328-8
29-6
50-24
/140
1 105-4
22-76
at 100° C.
„ 600" C.
„ 860° C.
,, 600° C.
,,1000° C.
„ 440° 0.
,, 440° C.
at 350° C.
„ 440° C.
,, 200° C.
„ 300° C.
„ 80° C.
A comparison of the values of w and m leads to the
follovring conclusions : —
(1) In the case of a very great number of substanceSj of
which only a few specimens are given in the table, the
two determinations agree, the slight difierences often
observed being evidently due to deviation of the sub-
stance from the state of a perfect gas. (2) In a consider-
able number of substances, physical evidence leads to a
multiple of the simplest number satisfying the chemical
conditions. This cannot be looked upon as a disagreement
between the methods, because, if a particular formula satis-
fies tho chemical conditions, any multiple of it -will neces-
sarily do so ; and indeed, in many of the cases we are now
considering, it is possible from chemical considerations to
justify the higher molecular weight after it has been sug-
gested, although such chemical considerations might not
in all cases have warranted its adoption without external
support. Thus, we are not without chemical evidence in
€22
[MOLECULE
favour of the formuloa Ho, CU, Oj, or even AloBr„ and FooCl^,
although chemists would probably have cottteuted them-
selves mth H, CI, O, AlBrj, and FeClj, had it not been for
the evidence of gas and vapour density, and certainly with-
out the latter no one would have thought of P^ As^, or Sg.'
(3) There are a number of substances in the case of
which there is an apparent disagreement between the
results of the two ways of determining molecular weight.
Such substances are said to have an anomalous gas or
vapour density. Tlie expression anomalous vapour density
ia sometimes applied to the case of such substances as
phosphorus and arsenic, but not very accurately. It
would be better to say that these substances have an
unexpected vapour density, because their complex molecular
formulte, while not clearly indicated by their chemical
character, are not at variance \vith any established law.
We shall therefore reserve the term " anomalous vapour
density " for those substances the molecular weight of
which as given by their vapour density is not reconcilable
with any formula which is chemically admissible. In
the case of some substances, such as the oxides of chlorine,
it has been shown that the discrepancy was due to errors
of observation, impure specimens having been used in
the experiments ; but there still remain many substances
having, in the sense above indicated, an anomalous vapour
density. These substances have therefore been examined
with special care, with the result of completely vindicating
the kinetic theory, and of disclosing a very interesting
and theoretically important kind of chemical change. We
.shall take, as instances of such .anomalous vapour densities,
the Eubstances in the last division of the table, and show
how the anomaly has in these ca-ses been explained.
Sal-ammoniac has the composition represented by the
formula N"H^C1. This formula agrees vsith all the chemical
actions of the substance and of all the substances in any
way related to it, but it does not agree with the results of
vapour density determinations. When sal-ammoniac is
heated it is converted into vapour or gas, and this vapour
or gas is reconverted into solid sal-ammoniac when it is
cooled. This looks exactly like the process of sublimation,
and it was universally supposed that the vapour given
off when sal-ammoniac is heated was really sal-ammoniac
vapovu". But its vapour density corresponds, not to the for-
mula NHjCl and the molecular weight 53'5, but to the
half of this. Now this formula does not admit of divi-
sion, and the explanation at once suggests itself, that
the vapour examined was not really the vapour of sal-
ammoniac, but of hydrochloric acid and ammonia gases,
the products of the decomposition of sal-ammoniac.
This would of course completely explain the apparent
anomaly ; each molecule NHjC'l dividing into two mole-
cules NHj and HCl, the gas from a given weight of sal-
ammoniac would of course contain twice as many molecules
and occupy twice the space which it would do if no such
decomposition had occurred. On this supposition the
mixed gases would remain uncomblned as long as the
temperature was above the decomposing point of sal-
ammoniac ; if the temperature fell below this point they
: ^ It ia unportant as a mattor of scientific history to note that this
.'i^^reoment of gas density and chemical molecular woight was first
indicated byGay-Lussac, who showed that the ratio of the densities of
two gases stood in a very simple arithmetical relation to the ratio of
their chomicaj egvivalents. Avogadro in 1811 brought forward his
famous hypothesis, that the number of vwlcailcs in a given volume of
gas ia independent of the nature of the gas, or that the densities of
gases (temperatdre and pressure being the same) are to one another
as the masses of their molecules. This hypothesis is now shown
to be in accordance with *.he ?:inetic theory of gas, and is known as
," Avogiulro's law." See Atcw, Trl. iii. p. 40, where a slight con-
^Tusion haa been caused by using the word " equivalent " Instead of
"molecule," and by not sufBcientlydistlngi.Ishing between the discovery
cf Oay-Lucsac and the hypothesis of Avogadrt-
would miite and reproduce sal-ammoniac. It was neces-
sary, however, to prove that this decomposition occirrs.
As has been shown above (p. 618), the rate of diffusion
of a gas depends upon its density. In this case the two
gases into which the substance may be supposed to break
up at the moment of volatilization differ con-siderably in
density ; we ought, therefore, to be able to effect partial
separation by means of diffusion, and it has been shown
that such partial separation actually does occur. Thus,
if we have hydrogen gas on one side of a porous dia-
phragm and volatilized sal-ammoniac on the other side,
we find after a time that, nrixed with the hydrogen on
the one side, we have what we may for shortness call sal-
ammoniac vapour — that is, a vapour which when cooled
forms solid sal-ammoniac — with an excess of ammonia,
which, being less dense than hydrochloric acid gas, has
diffused faster ; while on the other side, also mixed witk
hydrogen which has diffused through the diaphragm, we
have sal-ammoniac vapour with excess of hydrochloric acid,
the denser and more slowly diffusing gas. This of course
proves that> the decomposition has occurred, but it does
not prove that the vapour of sal-ammoniac consists entirely
of hydrochloric acid and ammonia mixed vn\}i one another.
That this in fact is not the case has been shown by an
ingenious experiment. The two gases were separately
raised to a temperature higher than that at which sal-am-
moniac volatilizes, and were then allowed to mix in a vessel
kept at the same temperature as the two gases. In this
vessel a delicate thermometer was placed, and it was found
that the mixing of the two gases was accompanied by a
small but very decided evolution of heat. This proves
that some chemical combination takes place, and that the
mixed gases must contain some vapour of NH,C1. More-
over, careful determinations of the vapour density of sal-
ammoniac prove that it is a little more than the mean
of the densities of ammonia and hydrochloric acid (a<
compared with air at the same temperature and pres-
sure, rOl instead of 0'9255 at 350°C.); and this increase
of densitj' on nuxing the hot gases is easily explained by
supposing that a small proportion is in the condition of
NH^Cl, while the most of the gas consists of separata
NHj and HCl molecules.
In a similar way it has been shown that the vapour of
oil of vitriol is a mixture of two vapours, — that of water,
H.,0, and that of sulphuric anhydride, SOj ; and that
sulphide of ammonium when volatilized breaks up into
two volumes of ammonia and one of sulphuretted hy-
drogen, (NH,)2S = 2NH3 -I- HjS. We find, therefore, that
in the former case, as in that of sal-ammoniac, t* = 2m,
and in the latter, w = Zm.
This pccnliar kind of decomposition is now known by the nam»
"dissociation." (See vol. v. pp. 476, 476.) In the cases we have
mentioned the substances undergo nearly complete dissociation at
the temperature at which they volatilize, and recombination takes
place when they are cooled and again assume the solid, or, as ia
the case of oil of vitriol, the liquid state. These substances »r>
therefore not suited for the illustration of the whole course of
dissociation. This haa been carefully studied in the case of somj
compounds, in which the dissociation is far from complete, at th >
boiling point of the substance, with the result that, if AH bo the
compound dissociating into the separate molecules A and B, wa
may represent the amount of dissociation as the ratio of the num-
ber of pairs of separate A and B molecules to the total number of
pairs o(a and B, both separate and combined. This ratio we ma/
call R, so that when dissociation is complete R = \.
(1) R increases as the temperature rises. (2) dRIdt (where t b
temperature) is a maximum when R = \. (3) The presence of exce?s
of cither A ot B diminishes the value of R. For instance, PCI5 is
nearly completely dissociated into PCI3 and CI, at 300° C. ; but if »
iart'e e.icess of PCI3 is mixed with tho vapour it is found to contaia
scarcely any CI,, so that dissociation is greatly diminished by tha
presence of excess of PCI,. These experimental results are capablo
of explanation on the kinetic theory of gas. if we adopt Pfaundler'?
hypothesis. This is, that for each case of dissociation there is a
M .O L — M O L
i623
limiting value for the internal Idnetic energy • of a molecule of AB.
If a molecule of AB, by encounters with other molecules or with
the wall of the vessel containing the gas, acquires a greater amount
of internal kinetic energy than this Umit, it at once Dreaks up into
A and B, so that in the gaseous mixtiu^ there are no molecules of
AB having more internal kinetic energy than the limit. Further,
if two molecules, one of A and one of B, meet one another with
such a velocity and with such an amount of intenial kinetic energy
that together the internal kinetic energy is less than the limit, they
will unite to form a molecule of AB. Thus the molecules with
peat internal kinetic energy will be separate molecules of A and
£ ; those with small internal kinetic energy will mostly be united as
AB. This hypothesis has been to a considerable extent worked out
And applied by Pfaundler and by Naumann, and the deductions
from it agree fairly well with the results of experiment ; but in some
points the theory has not been fully developed, and in some it does
not seem altogether to accord with observed facts. Some of these
difliculties have been mentioned above. We know enough of the
nature of dissociation to see that it belongs to the class of balana:d
chemical actions, in which a chemical change is reversible, and equili-
brium is kept up, with constant external conditions, by the two
opposite chemical changes taking place to an equal extent in a given
time. We can see that all such cases are explicable by the statistical
Tiuthod, but we cannot apply this method mathematically until we
know more of the intimate nature of the molecules and of the way
in which they act upon one another. In this discussion of dissocia-
tion we have looked specially at the cases in which -4, B, and AB
are all gaseous, because it was the question of anomalous vapour
densities which led us to treat of the subject. Dissociation also
occurs where one or two of the substances are solid or liquid.
We now see with what restrictions the method of vapour density
is applicable to the determination of molecular weight, and we can
understand more fully the example given in the article Chemistry,
vol. v. p. 469. It is there shown that acetic acid vapour does not
conform to the laws of Boyle and Charles until the temperature is
raised to about 250°, at the ordinary barometric pressure. At and
-above that temperature the vapour density corresponds to the formula
CjH^O^ At lower temperatures the density corresponds to a higher
molecular weight Now Playfair and Wanklyn determined the
vapour density at much lower temperatures than the ordinary boil-
ing point of acetic acid, by greatly diminishing the pressure of the
acetic acid vapour. This they accomplished by miiing it with a.
large quantity of hydrogen, so that the pressure duo to acetic acid
vapour formed only a small fraction of the total pressure. The
vapour density of acetic acid at the low temperatures at which they
worked was found to correspond very nearly with the formula
^4880^,. and, by comparing this result with what has been said
(p. 620) of the chemical evidence as to the molecular weight of acetic
acid, we may reasonably conclude that the molecule of acetic acid
at low temperatures is CjHjO,, and that as the temperature is raised
it undergoes dissociation, each molecule dividing into two of
CjHiOj. This is then a case where A and B are equal, and AA
divides ioto A + A. Another instance of the same kind is probably
to be found in peroxide of nitrogen (Chemisthy, p. 613), where
N3O4 divides into NO, + NOy Similarly, sulphur vapour has, at
temperatures below 500° C. , a density corresponding to the formula
Sg. This dissociates as the temperature rises until, about 1000° C. ,
the density corresponds to the formula Sj (Chemistry, p. 498).
We have now seen that chemistry receives great assistance in the
determination of molecular weight from physics, but this assistance
is almost entirely confined to the case of gases, or of substances
which can be volatilized. The phenomena of the diffusion of liquids
show us that there also there are independently moving particles ;
but the laws of liquid-diffusion have not been sufficiently gener-
alized to give us much help in the determinarion of the relative
masses of these particles. In liquids it is probable that the par-
ticles are very near each other, and that their shape and theix
mutual action, as well as their mass and the temperature, deter-
mine their rate of motion. t
In solids we have no independently travelling particles, and it is
perhaps scarcely correct to speak of a molecular structure of solids
at all Solids are no doubt composed of atoms, and those atoms
are evidently arranged in what may be called a tactical order.
When the solid is fused or dissolved or volatilized, it breaks into
molecules, each repetition of the pattern, if we may use the expres-
sion, being ready to become an independent thing under favourable
circumstances. But, while these potential molecules of solids can-
not perhaps be properly called molecules in a physical sense,* for
chemical purposes we may call them so, for they are the smallest
portions of the substance which fully represent it chemically, and,
as we have seen, this is the chemical molecule, the quantity which
should be represented by the formula. (A. C. B. )
MOLESKIN is a stout heavy cotton fabric of leathery
<onsistence woven as a satin twill on a strong warp. It
is finished generally either as a bleached white or as a slaty
<lrab colour, but occasionally it is printed in imitation of
tweed patterns. Being an exceedingly durable and econo-
mical texture, it was formerly much more worn by working-
men, especially outdoor labourers, than is now the case. It
is also used for gun-cases, carriage-covers, and several pur-
]ioses in which a fabric capable of resisting rough usage is
desirable.
MOLESWORTH, SraWnj^iAM (1810-1855), the eighth
bfironet,was born in London, 2.3d May 1810, and succeeded
to the extensive family estates in Devon and Cornwall in
1823. On the passing of the Reform Act of 1832 he was re-
"tumed to parliament, though only twenty-two years old, for
the eastern division of the county of Cornwall, to support the
ministry of Lord Grey. For some time he took little part
in the debates of the House of Commons; but in April 1835
he founded, in conjunction with Mr. Roebuck, the London
lieview, as an organ of the politidians known to the world
as " Philosophic Radicals." After the publication of two
volumes he purchased the Westminster Seeieio, and for some
time the united magazines were edited by him and J. S.
Mill. From 1837 to. 1841 Sir "William Molesworth sat for
the borough of Leeds, and during those years acquired con-
siderable influence in the House of Commons by his spee«Les
and by his tact in presiding over the select committee on
Transportation. From 1841 to 1845 he remained in private
life, occupying his leisure time in editing the works in Latin
and English of Thomas Hobbes of Malmesbury, a recreation
which cost him no less than JE6000. •• In the latter year he
* By internal kinetic energy is meant the kinetic energy of motion
of the parts of the molecule relatively to one another, in contradis-
tinction to the kinetic energy of motion of the molecule as a whole.
was returned for the borough of Southwark, and retained
that seat until his death. On his return to parliament he
devoted special - attention to the condition of the colonies,
and deUvered many speeches in favour of a reduction in
colonial expenditure and on their better administration.'
His argtiments on these questions changed the opinions of
the members of the House of Commons ; and the criticisms
of the daily pres.s, aided by the printing of his speeches, led
to the gradual acceptance of his views by the electors at
large. It was not, however, imtil many years afterwards that
he was allowed full opportunity for working out the difficult
problems connected with the government of Great Britain.
Office was conferred upon him in December 1852 by Lord
Aberdeen, but it was the minor post of directing the public
improvements and crown lands of his own country, and the
chief work by which his name was brought into prominence
at this time was the construction of the new Westminster
Bridge. At last, in July 1855, he was called to preside
over the Colonial Office, but unfortunately its duties were
no sooner entrusted to his care than he was cut off by
death (22d October 1855), to the universal regret of his
countrymen, for he had lived down the animosities of his
youth, and had attracted to himself the sympathies of
all thoughtful men. The influence which his views had
acquired, and still retain, may be judged from the fact thav
in 1878 the delegates of the Transvaal Government put
forward, as the chief argument for the withdrawal of the
English from the Transvaal, the substance of his speech on
the abandomnent of the Orange River Territory in 1854.'
A full pedigree of the lloliesworth family is printed in Sir John
Maclean's Trigg Minor, vol. i. ; the titles of his speeches and worka
It may be urged that the cleavage of crystals indicates that they
possess a molecular structure, but a tactical or pattern-like arrangement
of atoms may easily be supposed to present planes of easier separatioB,
without the assumption of really independent molecules.
624
M O L — M O L
may be found in the BiU. Com'uhicnsis, vols. i. and iiL . The name of
Sir Willi'im Molesworth is frequently mentioned in the biographies
of Mill, Cobden, Carlyie, Grote, and PanizzL
MOLFETTA, a city and seaport of Italy, in the -province
of Bari, 16 miles by rail nortli-nortli--west of Bari. From
the sea it presents a fine appearance with its white stone
houses and the remains of its turreted walla ; and there are
several buildings of considerable pretensions. The castle
was in the 14th centm-y the prison of Otho, duke of
Brunswick. The cathedral is dedicated to St Conrad.
Molfetta has weU-frequented markets, a small foreign trade
(6000 tons in 1881), and such industries as cotton and net
weaving, soap-boiling, and rope-spinning. The population
was 26,516 in 1871.
Molfetta (Melficta or Malfitum) was given by Charles T. to the
duke of Termoli in 1522, and during his lordship it was grievously
sacked by the French imder Lautrec. In 1631 Cesare Gonzaga took
the title of duke of Guastalla and prince of Molfetta ; but in 1640
the fief was sold to the Spinola family, a'nd in 1798 incorporated with
the royal domain. The bishopric holds directly of the papal see
MOLIEE.E (1622-1673), to give Jean Baptiste PoqueUn
the stage nanie which he chose, for some undiscovered reason,
to assume, w;- born in Paris, probably in January 1622.
The baptismal certificate which is usually, and almost with
absolute certainty, accepted as his is dated 15th January
1622, but it is not possible to infer that he was born jn
the day of his christening. The exact place of his birth
is also disputed, but it seems tolerably certain that he saw
the light iri a house of the Rue St Honors. His father
was Jean PoqueUn, an upholsterer, who, in 1631, succeeded
his ovTn uncle as "valet tapissier de chambre du roi." The
family of PoqueUn came from Beauvais, where for some
centuries they had been prosperous tradesmen. The
legend of their Scotch descent seems to have been finaUy
disproved by the researches of M. E. R^v&end du Mesnil.
The mother of MoUere was Marie Cress^ ; and on his
father's side he was connected with the family of Mazuel,
musicians attached to the court of France. In 1632
MoUfere lost his mother ; his father married again in 1633.
The father possessed certain shops in the covered HaUe de
la Foire, Saint Germain des Pr^s, and the biographers have
imagined that Molicre might have received his first bent
towards the stage from the spectacles offered to the hoU-
day people at the fair. Of his early education Uttio is
known ; but it is certain that his' mother possessed a Bible
and Plutarch's Lioes, books whicli an inteUigent child
would not faU to study. In spite of a persistent tradition,
there is no reason to beUeve that the later education of
MoU6re was neglected. " II fit ses humanitez au College
de Clermont," says the brief life of the comedian pubUshed
by his friend and fcUow-actor, La Grange, in the edition
of his works printed 'in 1682. La Grange adds that
MoUire " eut I'advantage de suivr.e M. le Prince de Conti
dans toutes ses classes." As Conti was seven years
younger than MoUire, it is not easy to understand how
MoUere came to be the school contemporary of the prince.
Among more serious studies the Jesuit fathers encouraged
their pupils to take part in ballets, and in later life
MoU6re was a distinguished master of this sort of enter-
tainment. According to Grimarest, the first writer who
published a Ufe of MoU6re in any detail (1705), he not
only acquired " his humanities," but finished liis " philo-
sophy " in five years. Ho left the College do Clermont in
1641, the year when Gassendi, a great ccjntomner of Aiis-
totle, arrived in Paris. The Logic and Hl/iics of Aristotle,
with Iiis Physics and Metaphysics, were the chief philoso-
phical toxt-books at the CoU(ige de Clermont. But when
he became the pupil of Gassendi (in company with Cyrano
de Bcrgerac, ChapeUo, and Hesnaut), Moliire was taught
to appreciate the atomic philosophy as taught by Lucretius.
There seems no doubt that MoUiro began, and almost or
qmte finished, a translation of the De Natura Ecrum.
According to a manuscript note of TraUage, pubUshed by
M. Paul LacroLx, the manuscript was sold by MoU^re's
widoY/ to a bookseller. His philosophic studies left a deep
mark on the genius of MoUfere. In the Jugemait de Pluton
sur les deux Parties des A'ouveaux Dialogues dcs Moris
(1G84), the verdict is "que MoUere ne parleroit point de
Philosophie." To " talk philosophy" was a favourite exer-
cise of his during his Ufe, and his ideas are indicated with
sufiScient clearness in several of his plays. There seems
no connexion between them and the opinions of " Moliero
lo Critique " in a dialogue of that name, pubUshed in Hol-
land in 1709. From his study of philosophy, too, he
gained his knowledge of the ways of contemporary pedants,
— of Pancrace the AristoteUan, of Marphorius the Carte-
sian, of Trissotin, "qui s'attache pour I'ordre au Peripa-
t(5tisme ", of Philaminte, who loves Platonism, of Belise,
who reUshes "les petits corps," and Armande, who loves
"les tombiUons." Grimarest has an amusing anecdote
of a controversy in which Molifere, defending Descartes,
chose a lay-brother of a begging order for umpire, while
Chapelle appealed to the same expert in favour of Gassendi.
His college education over, MoUere studied law, and there
is even evidence — that of tradition in Grimarest, and
of Le Boulanger de Chalussay, the libellous author of a
play caUed Elomire Hypochondre — to prove that he w?.s
actuaUy called to the bar. More trustworthy is the pass-
ing remark in La Grange's short biography (1682), " w,
soi-iir des ecoles de droit, il choisit la profession de come-
dien." Before joining a troop of haU-amate'ir comedian^-,
however, MoUere had some experience in his father's busi-
ness. In 1637 his father had. obtained for him the right
to succeed to his own ofiice as "valet tapissier de chambre
du roi." The document is mentioned in the inventory of
MoUfere's effects, taken after his death. When the king
traveUed the valet tapissier accompanied him to arrange
the furnitiu-e of the royal -quarters. There is very good
reason to beUeve (Loiseleur, Points Obscui-s, p. 94) that
MoUfere accompanied Louis XIII. as his valet tapissier to
Provence iu 1642. It is even not imjiossible that MoUere
was the young valet de chambre who concealed Cinq Mar.?
just before his arrest at Narbonne, 13th June 1642. But
this is part of the romance rather than of the history of
MoUere. Our next gUmpse of the comedian we get in a
document of 6th January 1643. MoUfere acknowledges
the receipt of money due to him from his deceased mother's
estate, and gives up his claim to succeed his father as " valet
de chambre du roi." On 28th December of the same year
we learn, again from documentary evidence, that Jean
Baptiste PoqueUn, with Joseph Bejard, Madeleine Bejard,
Genevieve Bejard, and others, have hired a tennis-court,
and fitted it up as a stage for dramatic performances. Tho
company caUed themselves L'lUustre TlieStre, illucire being
then almost a slang word, very freely employed by the
writers of the period.
We now reach a very important point in tho private
history of MoUire, v/hich it is necessary to discuss at some
length in defence of the much maligned character of a
great writer and a good man. MoUere's connection with
tlie family of Bejard brought him much unhappiness.
Tho father of this family, Joseph Bi^jard (he elder, was a
needy man with eleven children at least. His wife's name
was Marie Herve. The most noted of his children, com-
panions of Molicre, were Joseph, Madeleine, Genevieve, and
Armande. Of these, Madeleine was a woman of great
talent as an actress, and MoUirc's friend, or perhaps mis-
tress, through all the years of his wanderings. Now, on
14th February 1662 (for wo must here leave the chrono-
logical order of events), MoUere married Armande Claire
Elisabeth Gr&inde Bejard. His enemies at that time,'
M O L I E K E
625
and a nvunber of his biographers in our own day, have
attempted to prove that Armande B6jard was not the sister,
but the daughter of Madeleine, and even that Moliere's
wife may have been his own daughter by Madeleine
Bijard. The arguments of M. Arsine HoussayS in sup-
port of this abominable theory are based on reckless and
ignorant confusions, and do not deserve criticism. But
the system of M. Loisele'ir is more serious, and he goes
no further than the idea that Madeleine was the mother
of Armande. This, certainly, was the opinion of tradition,
an opinion based on the slanders of Montfleury, a rival of
Moliere's, on the authority of the spiteful and anonymous
author of La Fameiite Comedienne (1688), and on the
no less libellous play, £lomiri Sypochondre. In 1821
tradition received a shock, for Beflfara then discovered
Moliere's "acte do mariage," in which Armande, the bride,
is spoken of as the sister of Madeleine B^jard, by the same
father and mother. The old scandal, or part of it, was
revived by M. Foumier and M. Bazin, but received another
blow in 1863. M. Soulie then discovered a legal document
of 10th March 1643, in which the widow of Joseph B^jard
renounced, in the name of herself and her children, his
inheritance, chiefly a collection of unpaid bills. Now in
this document all the children are described as minors, and
among them is " une petite non encore baptisee." This little
girl, still not christened in March 1643, is universally
recognized as the Armande B^jard afterwards married by
Molifere. We reach this point, then, that when Armande
was an infant she was acknowledged as the sister, not as the
daughter, of Madeleine B^jard. M. Loiseleur refuses, how-
ever, to accept this evidence. Madeleine, says he, had
already become the mother, in 1638, of a daughter by
Esprit Raymond de Moirmoron, comte de Modtoe, and
chamberlain of Gaston due d'Orl^ns, brother of Louis
XIIL In 1642 Modine, who had been exiled for political
reasons, "was certain to return, for EicheUeu had just
died, and Louis XIIL was likely to follow him." Now
Madeleine was again — this is M. Loiseleur's hypothesis —
about to become a mother, and }i Modine returned, and
learned this fact, he would not continue the liaison, still
less would he marry her, — which, by the way, he could not
do, as his wife was still alive. Madeleine, therefore,
induced her mother to acknowledge the little girl as her
own child. In the first place, all this is pure unsupported
hypothesis. In the second place, it has always been denied
that B^jard's wife could have been a mother in 1643, owing
to her advanced age, probably fifty-three. But M. Loise-
leur himself says that Marie Herve was young enough to
make the story " suflBciently probable." If it was probable,
much more was it possible. M. Loiseleur supports his
contention by pointing out that two of the other childien,
described as legally minors, were over twenty-five, and that
their age was understated to make the account of Armande's
birth more probable. Nothing is less likely than that
Mod^ne would have consulted this document to ascertain
the truth about the parentage of Armande, yet M. Loise
leur's whole theory rests on that extreme improbability.
It must also be observed that the date of the birth of
Joseph B^jard is unknown, and he may have been, and
according to M. Jal (Dictionnaire Critique, p. 178) must
have been, a minor when he was so described in the do:u-
taent of 10th March 1643, while Madeleine had only parsed
her twenty-fifth birthday, her legal majority, by iwo months;
This tiew of Joseph's age is supported by Bouquet (Jloliere
A Rouen, p. 77). M. Loi3bieiU''3 only other proof is that
Marie Herv^ gave Armande a respectable dowry, and that,
as we do not know whence the money came, it must have
come from Madeleine. The tradition in Grimarest, which
makes Madeleine behave en femme furieiise, when she heard
of the marriage, is based on a juster appreciation oi, the
1&— 23
character of women. It will be admitted, probably, that
the reasons for supposing that Moliire espoused the daughter
of a woman who had been his mistress (if she had been his
mistress) are flimsy and inadequate. The affair of the
dowry is insisted on by M. Livet {La Fameuse Comedienne,
reprint of 1877, p. 143). But M. Livet explains the dowry
by the hypothesis that Armande was the daughter of
Madeleine and the comte de Mod^ne, which exactly con-
tradicts the theory of M. Loiseleur, and is itself contra-
dieted by dates, at least as imderstood by M. Loiseleur.
Such are the conjectures by which the foul calumnies of
Moliere's enemies are supported in the essays of modern
French critics.
To return to the order of events, Molifere passed the
year 1643 in playing with, and helping to manage, the
Theatre Illustre. The company acted in various tennis-
courts, with very litlje success. Moliire was actually
arrested by the tradesman who supplied candles, and the
company had to borrow money from one Aubrey to release
their leader from the Grand Chatelet (13th August 1645).
The process of turning a tennis-court into a theatre was
somewhat expensive, even though no seats were provided
in the pit. The troupe was for a short time under the
protection of the due d'Orl^ans, but his favours were not
lucrative. The due de" Guise, according to some verses
printed in 1646, made Molifere a present of his cast-ofif
wardrobe. But costume was not enough to draw the
public to the tennis-co\irt theatre of the Croix Noire,
and empty houses at last obliged the Th^tre Illustre to
leave Paris at the end of -1646.
"Nul animal vivant n'entia dans notre salle," says the
author of the scurrilous play on Molifeie, Slomire Uypo-
chondre. But at that time some dozen travelling companies
found means to exist in the provinces, and Moliire deter-
mined to play among the rural towns. The career of a
strolling player is much the same at all times and in all
countries. The Roman Comique of Scarron gives a vivid
picture of the adventures and misadventures, the difficulty
of transport, the queer cavalcade of horses, ruules, and
lumbering carts that drag the wardrobe and properties,
the sudden metamorphosis of the tennis-court, where the
balls have just been rattling, into a stage, the quarrels with
local squires, the disturbed nights in crowded country inns,
all the loves and wars of a troupe on the march. Perrault
tells us. what the arrangements of the theatre were in
Moliere's early time. Tapestries wsfe hung round the
stage, and entrances and exits were made by struggling
through the heavy curtains, which often knocked aS the
hat of the comedian, or gave a strange cock to the helmet
of a warrior or a god. The lights were candles stuck in
tin sconces at the back and sides, but luxury sometimes
went so far that a chandelier of four candles was suspended
from the roof. At intervab the candles were let do^m by
a rope and pulley, and any one within easy reach snuSed
them with his fingers. A flute and tambour, or two
fiddlers, supplied the music. The highest prices were paid
for seats in the dedans (cost of admission fivepence) ; for
the privilege of standing up in the pit twopence-halfpenny
was the charge. The doors were opened at one o'clock,
the curtain rose at two.
The nominal director of the Th^dtre Illustre in ths
provinces was Du Fresne ; the most noted actors were
Moliere, the Bejards, and Du Pare, called Gros Ren^. I»
is extremely difficult to follow exactly the line of march of
the company. They played at Bordeau.x, for example, but
the date of this performance, when Moliire (according to
Montesquieu) failed in tragedy and was pelted, is variously-
given as 1644-45 (TraUage), 1647 (Loiseleur), 1648-58
(Lacroii). Perhaps the theatre prospered better eUs-
where than in Paris, where the streets were barricaded in
026
M O L I E R E
tncsc early days ot tlie war of the Fronde. <Vo find
Moliere at Nantes in 1C4S, at Fontenay-lc-Com;,>to, and
in tlie spring of 1G49 at Agen, Toulouse, and probably at
Angouliinio and Limoges. In January IGOO they played
at Narbonno, and between 1G50 and 1G53 Lyons was the
headquarters of the troupe. In January 1G53, or perhaps
IGf).'), Moliere gave L'Elourdi at. Lyons, the fir.it of his
finished pieces, as contrasted with the slight farces with
which he generally diverted a country audience. It would
be interesting to have the precise date of this piece, but
La Grange (1GS2) says that "in 1G53 Molifere went to
Lyons, where ho gave his first comedy, L'litourdi," while
in his Ueijistre La Grange enters the year as 1655. At
Lyons De Brio and his wife, the famous Mile, de Erie,
entered the troupe, and Du Pare married marquise de Gorla,
better known as Jllle. du Pare. The libellous author of
La Fameuse Comedienne reports that Sfolifere's heart was
the shuttlecock of the beautiful Du Pare and De Brie, and
the tradition has a persistent life. Moliure's own opinion
t)f the ladies and men of his company may be read be-
tween the lines of his Impromptu de Versailles. In 1653
.Prince de Conti, after many political adventures, was
(residing at La Grange, near Pezenas, in Languedoc, and
'chance brought him into relations with his old school-
fellow Moliere. Conti had for first gentleman of his bed-
cliamber the abbiS Daniel de Cosnac, whose memoirs now
ithrow light for a moment on the fortunes of the wander-
ing troupe. Cosnac engaged the company " of Molifere and
'of La Bejart;" but another company, that of Cormier, nearly
intercepted the favour of the prince. Thanks to the resolu-
tion of Cosnac, Moliere was given one chance of appearing
on tiie private theatre of La Grange. The e.xcellence of
Lis acting, the splendour of the costumes, and the insist-
ence of Cosnac, and of Sarrasin, Conti's secretary, gained
the day for Moliere, and a pension was assigned to his
company (Cosnac, Memoires, i. 128, Paris, 1852). As
Cosnac proposed to pay Moliere a thousand crowns of his
|own money to recompense him in case he 'was supplanted
Iby Cormiei', it is obvious that his profession had become
sufficiently lucrative. In 1654, during the session of the
estates of Languedoc, Jloliire and his company played at
Iilontpellier. Hero Moliere danced in a ballet (Le Ballet
<les Incompatibles) in which a number of men of rank took
part, according to the fashion of the time. Moliere's own
7-6les were those of the Poet and the Fishwife. The sport
ot the little piece is to introduce opposite characters,
dancing and singing together. Silence dances with six
women. Truth wlJi four courtiers. Money witli a poet,
and so forth. Wliether tlie ballet, or any parts of it, are
by Moliere, is still disputed (La Jennesse de Moliere, suiiie
till Ballet des Incompatibles, P. L. Jacob, Paris, 1858). In
April 1G55 it is certain that the troupe was at Lyons,
wliere they met and hospitably entertained a profligate
buffoon, Cliarlcs d'Assoucy, who informs the ages that
Moliere kept open house, and "vne table lien (/arnie."
November 1655 found Moliere at Pdzenas, where the
estates of Languedoc were convened, and where local
tradition points out the barber's chair in which the poet
used to sit and stu<ly character. The longest of j\Ioli6re's
extant E'ltographs is a receipt, dated at Pezenas, 4th Feb-
ruary 1G5G, for 6000 livres, granted by the estates of
Languedoc. Tlii." year was notable for the earliest repre-
fentation, at Eezieri, oJ >foliire's second finished comedy,
the Dcpit Amoureux. Conti riow v.-:lhdre\ir to Paris, and
began to "make his soul," as the Insh soy. Almost liis
first act of penitence was to discard i\Io!iire'i; troupe (1057),
which consequently found that the liberality of iko estates
of Languedoc was dried up for ever. Conti's relations
with Moliere must have defin'lively cbscd long before IGCG,
v/ben the now pious prince jjot; a treatise cjrainst the
stage, and Especially cnarged Lis old schoolfellow iritJi
keeping a new school, a school of atheism {Traite de la
Comidie, p. 24, Paris, 1G66). Moliere was now (1657)
independent of princes r.nd their favour. He went on a
new circuit to Nismes, Orange, and Avignon, Avhere he met
another old class-mate, Chapelle, and also encountered tl!e
friend of his later life, the painter Mignard. After a later
stay at Lyons, ending with a piece given for the benefit
of the poor on .27th February 1658, Moliere passed to
Grenoble, returned to Lyons, and is next found in Rouen,
where, we should have said, the The.';tre Illustre had played
in 1643 (F. Bouquet, La Tronpe da Moliere ch liouen,
p. 90, Paris, 1880). At Rouen Moliere must have made
or renewed the acquaintance of Pierre and Thomas Cor-
neille. His company had played pieces by Corneille at
Lyons and elsewhere. The real business of the comedian
in Rouen was to prepare his return to Paris. "After
several secret journeys thither he was fortunate enough to
secure the patronage of Monsieur, the king's only brother,
who granted him his protection, and permitted the company
to take his name, presenting them as Lis servants to tlie
king and the queen-mother" (Preface to La Grange's
edition of 1682). The troupe appeared for the first time
before Louis XIV. in a theatre arranged in the old Louvre
(24th October 1658).
Jlolifere was now thirty-six years of age. He had gained
all the experience that fifteen years of practice could give.
He had seen men and cities, and noted all the humours ot
rural and civic France. He was at the head of a company
which, as La Grange, his friend and comrade, says, '" sin-
cerely loved him." He had the unlucrative patronage of
a great prince to back him, and the jealousy ot all play-
wrights, and of the old theatres of the Hotel de Bourgogne
and tlie Marais, to contend against. In this .struggle we
can follow him by aid of the Rcgistre of La Grange (a
brief diary of receipts and payments), and by the help of
notices in the rhymed chronicles of Loret.
The first appearance of Moliere before the king was all
but a failure. Nicomede, by the elder Corneille, was the
piece, and we may believe that the actors of the Hotel da
Bourgogne, who were present, found much to criticize.
^\Tien the play was over, Moliere came forward and asked
the king's jiermission to act "one of the little pieces with
which Le Lad been used to regale the provinces." The
Dodeiir Amourctix, one of several slight comedies admitting
of much "gag," was then performed, and "diverted as
much as it surprised the audience." The king commanded
that the troupe shoiJd establish itself in Paris (Preface, ed.
1682). The theatre assigned to the company was a «a//«
in the Petit Bourbon, in a line with the jiresent Rue du
Louvre. Some Italian players already occupied the hou.so
on Tuesdays, Fridays, and Sundays ; the comjiany of
^Moliere jilayed on the other days. The first piece played
in the new house (3d Nov. 1658) was L'Ltourdi. La
Grange says the comedy had a great success, producing
seventy pistoles for each actor. The success is admitted
even by the spiteful author of £lomire N^iocliondre (Paris,
' "Jo jouii I'Etourdi, qui fiit unc mervcillo."
The success, however, is attributed to tLe farcical element
in the i>lay and the acting — the cuckoo cry of Molifere's
detractors. The original of L'Btovrdi is the Itarian comedy
(1G29) L'Inameriito, by Nicol6 Barbieri detto Bcltrame;
Moliere pushed lather far his right to "take his own
wherever Le found it." Had he wri'ten nothing more
original, the contemporary critic of X j'cs'in de Picm
might have said, not -untruly, that ho J.nly excelled in
steahng pieces from the Italians. The piece is conventional ;
the stock characters of the prodigal son, the impudent
valet, the old father occupy the stage. But the dia'ogua.
M O L I E R J:
en
las amazing rapidity, and the vivacity of M. Coquclin in
JMascarille still makes L'£'tourdi a favomite on the stage,
(though it cannot be read with very much pleasure. The
next piece, new in Paris, though not in the provinces, was
the Dcpit Amoureiix (first acted at Beziers, 1G5G). The
play was not less successful than L'Eicmrdi. It has two
parts, one an Italian imbroglio; the other, which alone
keeps the stage, is the original work of Moliire, though, of
course, the idea of amanilum irss is as old as literature.
"Nothing so good," says Mr. Saintsbury, "had yet been
seen on the French stage, as the quarrels and reconciliations
of the quartette of master, mistress, valet, and soubrette."
Even the hostUe Le Boulanger de Chalussay {Elomire
Hypochondre) admits that the audience was much of this
opinion —
" Et do tons les c6tes chacon cria tout haut,
' C'est la faire et jouer lea pieces comme il faut." " \
The same praise was given, perhaps even more deservedly, to
Lea Prideuses Ridicules {X^t^i November 1659). Doubtshave
been raised as to whether this famous piece, the first true
comic satire of contemporary foibles on the French stage,
was a new play. La Grange calls it piece nouvelle in his
Seffisire, but, as he enters it as the third piece nouvelle,
he may only mean that, like L'JEtourdi, it was new to
Paris. The short life of 1682, produced under La Grange's
care, and probably written by Marcel the actor, says the
Precieuses was " made " in 1659. There is another contro-
versy as to whether the ladies of the Hotel Rambouillet,
or merely their bourgeoises and rastic imitators, were laughed
at. Manage, in later years at least, professed to recognize an
attack on the over-refinement and aifectation of the original
and, in most ways, honoxu-able precieuses of the Hotel Ram-
bouillet. But Chapelle and Bachaumont had discovered
provincial precieuses, hyper-a^sthetic literary ladies, at Mont-
pellier before Moheru's return to Paris ; and Furctifcre,
in the Soman Bourgeois (1666), found Paris full of middle-
class precieuses, who had survived, or, like their modem
counterparts, had thriven on ridicule. Another question
is — Did Moliire copy from the earlier Precieuses of the
abb^ de Pure t This charge of plagiarism is brought by
Soniaize, in the preface to his Veriiables Precieuses. De
Pure'o work was a novel (1656), from which the Italian
actors had put together an acting piece in their manner,
that is, a thing of "gag," and improvized speeches. The
reproach is interesting only because it proves how early
Moliiro found enemies who, like Thomas Corneille in 1659,
accused him of being skilled only in farce, or, like Somaize,
charged him with literary larceny. These were the stock
criticisms of Moliere's opponents as long as he lived. The
success of the Precieuses Pidicnles was immense ; on one
famous occasion the king was a spectator, leaning against
the great chair of the dying Cardinal Mazarin. The play
can never cease to please while literary affectation exists,
and it has a comic force of deathless energy. Yet a modern
reader may spare some sympathy for the poor heroines,
,who do not wish, in courtship, to "begin vrith marriage,"
^but prefer first to have some less formidable acquaintance
.with tlieir wooers. Moliere's next piece was less important,
and more purely farcical, Sganarelle ; ou le Cocu Imagin-
JniVe (2Sth May 1660). The public taste preferred a work
of this light nature, and Sganarelle was played every year
as long as Molitre lived. The play was pirated by a man
who pretended to have retained all the words in his memory.
The counterfeit copy was published by Ribou, a double
injury to Molifere, as, once printed, any company might act
the play. With his habitual good-nature, Molifere not only
allowed Ribou to publish later works of his, but actually
lent money to that knave (Souli6, Recherches, p. 287).
On 11th October 1660 the Theatre du Petit Bourbon
iiras demolished by the superintendent of works, without
notice given to the company. The king gavo Moliere the
Salle du Palais Royal, but the machinery of the old theatre
was mahciously destroyed. Meanwhile the older companies
of the Marais and the Hotel de Bourgogne attempted to
lure away MoUere's troupe, but, as La Grange declares
(Pegisire, p. 26), "all the actors loved their chief, v/ho
united to extraordinary genius an honourable character
and charming manner, which compelled them all to protest
that they would never leave him, but always share his for-
tunes." AVhile the new theatre was being put in order,
the company played in the houses of the great, and before
the king at the Louvre. In their new house (originally
built by Richelieu) Moliire began to play on 20tii January
1661. Molifere now gratified his rivals by a failure. Don
Garcie de Navarre, a heavy tragi-comedy, which had long
lain among his papers, was first represented on 4 th February
1661. Either Molifere was a poor actor outside comedy,
or his manner was not sufficiently "stagy," and, as he
says, " demoniac," for the taste of the day. His opponents
were determined that he could not act in tragi-comedy, and
he, in turn, burlesqued their pretentious and exaggerated
manner in a later piece. In the Precieuses (sc. ix.) Moliere
had already rallied " les gi'ands comedicns " of the Hotel
Bourgogne. " Les autres," he makes ilascarille say about
his own troupe, " sont des ignorants qui r^citent comma
Ton parle, ils ne savent pas faire ronfler les vers." All this
was likely to irritate the grands comediens, and their friends,
who avenged themselves on that unfortunate jealous prince,
Don Garcie de Navarre. The subject of this unsuccessful
drama is one of many examples which show how Moliere's
mind was engaged with the serious or comic aspects of
jealousy, a passion which he had soon cause to know most
intimately. Meantime the everyday life of the stage went
on, and the doorkeeper of the Theatre St. Germain was
woimded by some revellers who tried to force their way
into the house (I^a Grange, Eegistre). A year later, an
Italian actor was stabbed in front of Moliere's house, where ■
be had sought to take shelter (Campardou, Kouvelles Pieces,^
p. 20). To these dangers actors were peculiarly subject ;
Moliere himself was frequently threatened by the marquises
and others whose class lie ridiculed on the stage, and there
seems even reason to believe that there is some truth in
the story of the angry marquis who rubbed the poels head'
against his buttons, thereby cutting his face severely. The
story comes late (1725) into his biography, but is supported
by a passage in the contemporary play, Zeliinle (Paris,
1663, scene viii.). Before Easter, Moliere asked for two
shares in the profits of his company, one for himself, and
one for his vnie, if he married. That fatal step was already
contemplated (La Grange). On 24th June he brought
out for the first time L'Hcole des Maris. The general idea
of the piece is as old as Menandcr, and Moliere was
promptly accused of pilfering from the Adclphi of Terence.
One of th.% ficelles of the comedy is borrowed from a story,
as old, at least, as Boccaccio, and still amusing in a novel
by Charles de Bernard. It is significant of Moliere's talent
that the grotesque and bafllcd paternal wooer, Sganarelle,
like several other butts in Moliere's comedy, does to a
certain extent win our sympathy and ]>ity as well as our
laughter. The next new piece was Les Faschevjr, a comklie-
ballet, the Comedy of Bores, played before the king at
Fouquet's house at Vaux le Vicomte (August 15-20, 1661).
The comedians, without knowing it, were perhaps the real
" fascheux " on this occasion, for Fouquet was absorbed in
the schemes of his insatiable ambition {Quo non asceudam ?
says his motto), and the king was organizing the arrest
and fall of Fouquet, his rival in the affections of La
Valliere. The author of the prologue to Les Fascheux,
Pellisson, a friend of Fouquet's, was arrested along with
the superlatcndent of fmanc.e. Fellisson's prologue an4
628
M OL I E R E
■name were retained in later editions. In the dedication
to the king Moliere says that Louis suggested one scene
(that of tlie Sportsman), and in another place he mentions
that the piece was ^vl'itten, rehearsed, and. played in a
fortnight. The fundamental idea of the play, the inter-
ruptions by bores, is suggested by a satire of Regnier's,
and that by a satire of Horace. Perhaps it may have been
the acknowledged suggestions of the king which made
gossips declare that iloliire habitually worked up hints
and mcniotVcs. given him by persons of quality {Nouvelhs
NouvcUes, 1663).
In February 1662 Moliere married Armande B^jard.
The date is given thus in the Eegistre of La Grange :
" JIardy 14, Lea Visignnaires, L'liicol des M.
Part. Visite chez M° d'Equeuilly."
And on the margin he has painted a blue circle, Ms way of
recording a happy event, with the words, " mariage de M.
de Moliere au sortir de la Visite." !M. Loiseleur gives the
date in one passage as 29th February, in another as 20th
February. But La Grange elsewhere mentions the date
as "Shrove Tuesday," which was, it seems, l-tth February.
Elsewhere M. Loiseleur makes the date of the marriage a
vague day " in January." The truth is that the marriage
contract is dated 23d January 1662 (Soulie, Doctiments, p.
203). Where it is so difficult to establish the date of the
marriage, a simple fact, it must be infinitely harder to dis-
cover the truth as to the conduct of Madame Moliere. The
abominable assertions of the anonymous libel, Les Intrigues
de Moliere et celles de sa Femme; ou la Fameuse Comedienne
( 1 6SS), have found their way into tradition, and are accepted
by many biographers. But M. Livet and M. Bazin have
proved that the alleged lovers of JMadame Moliere were
actually absent from France, or from the court, at the
time when they are reported, in the libel, to have conquered
her heart. A conversation between Chapelle and Moliere,
in which the comedian is made to tell the story of his
^ wrongs, is plainly a mere fiction, and is answered in
Grimarest by another dialogue between Moliere and Eohault,
in which Moliere only complains of a jealousy which he
knows to be unfounded. It is noticed, too, that the con-
temporary assailants of Moliere counted him among jealous,
but not among deceived, husbands. The hideous accusation
brought by the actor ilontfleury, that Moliere had married
his own daughter, Louis XIV. answered by becoming the
godfather of Moliere's child. The king, indeed, was a
firm friend of the acto;-, and, when Moliere was accused of
impiety on the production of Don Juan (1665), Louis gave
him a pension. We need not try to make Madame Moliere
a oertu, as French ladies of the th- atre say, but it is certain
that the charges against her a'-e unsubstantiated. It is
generally thouglit that Molitro drew her portrait in Le
Boxirgeois Gentilhomme, acte iii. sc. ix., " elle est capri-
cieuse, mais on souflVe tout des Belles."
From 1662 onwards Jloliire suffered the increasing
hatred of his rival actors. La Grange mentions the visit
of Floridor and JMontfleury to the queen-mother, and
their attempt to obtain equal favour, " la troupe de Jloliere
leur donnant bcaucoup do jalouzie" (12th August 1662).
On 26th December was played for the first time the
admirable £mle des Femmes, which provoked a literary
war, and caused a shower of " paper bullets of tlie brain."
The innocence of Agnes was called indecency ; the sermon
of Arnolphe was a deliberate attack on Christian mysteries.
We have not the space to discuss the religious ideas of
JIoli6re ; but both in Vtlcole des Fcmmes and in Don Juan.
ho docs display a bold contempt for the creed of " boiling
chaldrons" and of a physical hell. A brief list of tlie
plays and pamplilets provoked by L']J!cole des Feimnes is all
we can offer in this place.
December 26, 1662.— .&o7<! da Fcmmcs.
febriury 9, 1663. — ycuvcUa KouvelL^ by Dc Vise. MoliJre ia
accused of pilfering, from iStraparola.
June 1, 1660. — Jloliere's own piece, CrUiqiu de TEcole des
Femmcs. In this play Moliure retorts on the critics, and especially
on his favourite butt, the critical marquis.
August 16G3. — Zilinde, a play by J)e Vise, is printed. ' The scene
is in the shop of a seller of lace, where persons of quality meet, and
attack the reputation of "ilomu-e," that is, MoUere. He steals
from tlie Italian, the Spanish, from Furetiere's Francion^ *' il Ut tous
lc-3 vieux bouquius," lie insults the nohlessc, he insults Ciu'istianity,
and 50 foi-th.
November 17, 1G63. — Portrait dii Pcintrc is printed, — an attack
on Uoliere by Boursault. This piece is a detailed criticism, by
several persons, of L'£coh des Fcmmcs. It is pronounced duD,
vulgar, farcical, obscene, and (what chiefly vexed Moliere, who knew
the danger of the accusation) impious. Perhaps the only biogi-aph-
ical matter we gain from Boursault's play is tho hitercsting fact
that Jloliere was a tennis-plaj-er. On 4th November 1063 Moliere
replied with L' Impromptu dc Versailles, a witty and merciless
attack on his critics, in which Boursault was mentioned by name.
The actors of the H6tel de Bourgogne were parodied on the stage,
and their art was ridicided.
The next scones in this comedy of comedians were : —
NovembcrSO. — ThuPanlgyriquc del' J&colc des Fcmmcs, byKobinet.
December 7. — Itepoiise a VImpromptu; ou la Veiigcaiicc des Mar-
quis, by De Vise.
January 19, 1664. — VImpromptu de VHdtel de , Condi. It is a
reply by a son of Montflcury. ^
March 17, 1664. — La Guerre Comiquc; oa Defense de TEcole des
Fcmmcs.
, 1664. — Letlre sur Ics .Affaires du TlUitre, published in Divcrsitd
Galantes, by the author of Zdlinde.
In all those quarrels the influence of Corneille was
opposed to Moliere, while his cause was espoused by
Boileau, a useful ally, when " les comediens et les auteurs,
depuis le cidre [Corneille ?] jusqu'k I'hysope, sont enable-
ment animes contre lui" {Impromptu de Versailles, scene v.).
Jloliere's next piece was Le Mariage Force (loth Feb-
ruary 166-1), a farce wth a ballet. The comic character
of the reluctant bridegroom excites contemptuous pity,
as weU as laughter. From the end of April till 22d May
the troupe was at Versailles, acting among the picturesque
pleasm'es of that great festival of the king's. The Prineesse
(Ci'lide was acted for the first time, and the three first
acts of Tartu fe were given. Moliere's natural hatred of
hypocrisy had not been diminished by the charges of blas-
phemy ^vhich were showered on him after the Fcole dea
Femmes. Tartuffe made enemies everj-where. Jansenists
and Jesuits, like the two marquises in L' Impromptu de
Versailles, each thought the others were armed at. Five
years passed before Jlolitre got permission to jjlay the
whole piece in public. In the interval it was acted before
jMadame, Condc, tlie legate, and was frequently read by
Moliere in private houses. The Gazette of 17th May 1664
(a paper hostile to Moliere) says that the king thought the
piece inimical to religion. Louis was not at that time
on good terras with the devols, whom his amours scandal-
ized; but, not impossibly, the queen-mother (then suffering
from her fatal malady) disliked the play. A most violent
attack on Moliere, " that demon clad in human flesh," was
■\viitten by one Pierre PiOuUe (Le lioi/ Glorieux au Monde,
Paris, 1664). This fierce pamphlet was suppressed, but
the king's own co])y, in red morocco with the royal arms,
remains to testify to tho bigotiy of the author, who was
cur6 of Saint PHarthiJIcmy. According to Eoulld, Moliere
deserved to be sent through earthly to eternal fires. Tho
play was prohibited, as .we have seen, but in August 1665
the king adopted Moliere's troupe as his servants, and gave
them tho title of "troupe du roy." This, however, did not
cause Moliere to relax his efforts to obtain permission for
Tartu fe (or Tartv/e, or Tartvjie, as it was variously spelled),
and his perseverance was at loiiglli successfuL That his
thoughts were busy with contcmjiorary hyjiocrisy is proved
by certain scenes in one of his greatest pieces, tho Fcsii.i
dc Pierre, or Don Jtian (15th Febrnary 1665). The legei'.il
of Don Juan was familiar already on the Spanish, Italion,
M O L I E R E
629
and FfoiicTr stares, McircrTT^iaac rtanewthing: terriWs
and roniantxr. in its portrait of un grand seigneur mauvais
Jiomme, modem inils s.-gsested substitution of la lutmanite
for religion, comic, even among his comedies, by the mirth-
ful character of Sganarelle. The piece filled the theatre,
but was stopped, probably- by authority, after Easter. It
was not printed by Jloliere, and even in 16S2 the publi-
cation of the full text was not permitted. Happily the
copy of De la Kegnie, the chief of -the police, escaped
obliterations, and gave us the fuU scene of Don Juan and
the Beggar. The piece provoked a virulent criticism
{Observations sur h Fesiin de Pierre, 1665). It Is allowed
that Mohere has some farcical talent, and is not unskilled
as a plagiarist, but he "attacks the interests of Heaven,"
"keeps a school of infidelity," "insults the king," "cor-
rupts virtue," "oflFends the queen-mother," and so forth.
Two replies were published, one of which is by some critics
believed to show traces of the hand of Moli^re. The king's
reply, as has been shown, was to adopt Moliere's company
as his servants, and to pension them. L' Amour Medecin,
a light comedy, appeared 22d September 1665. In this
piece Moliire, for the second time, attacked physicians.
'In December there was a quarrel with Eacine about his
play of Alexandre, which he treacherously transferred to the
Hotel de Bourgogne. June 4, IGCG saw the first repre-
eentation of that famous play, Le Misatithrope {ou L'Aira-
hiliaire Amoureux, as the original second title ran). Tiis
IJiece, perhaps the masterpiece of Moliere, was more suc-
cessful with the critics, with the court, and with posterity
than >vith the pubUc. The rival comedians callod it " a
new style of comedy," and so it was. The eternal passions
and sentiments of human nature, modified by the influence
of the utmost refinement of civilization, were the matter of
the piece. The school for scandal kept by Celimene, with
its hasty judgments on all characters, gave the artist a
,wide canvas. The perpetual strife between the sensible
optimism of a kindly man of the world (Philinte) and the
soiva indigndtio of a noble nature soured (Alceste) sup-
plies the intellectual action. The humours of the joyously
severe CeLimijne and of her court, especially of that death-
less minor poet Oronte, supply the lighter comedy. Boileau,
Lessing, Goethe have combined to give this piece the
highest rank even among the com.edies of Moliere. As to
the " keys " to the characters, and the guesses about the
original from whom Alceste was dra\^ii, they are as value-
less as other contemporary tattle.
A briefer summary must be given of the remaining years
of the life of Moliere. The attractions of Le Misanthropic
were reinforced (6th August) by those of the Medecin
Malgre Lui, an amusing farce founded ou an old fabliau.
In December the court and the comedians went to Saint
Germain, where, among other diversions, the pieces called
MUicerte, La Pastorale Comique (of which Moliure is said
to have destroyed the MS.), and the charming little piece
Le Sicilien, were performed. A cold and fatigue seem to
have injiired the health of Jlolierc nd we now hear of
the consumptive tendency which was cruelly ridiculed in
jSlomire Uypocliondre. Moliere was doubtless obliged to
see too. much of the distracted or pedantic physicians of an
age when medicine was the battlefield of tradition, super-
stition, and nascent chemical science. On 17th April
1667 Eobinet, the rhyming gazetteer, says that the life of
Moliere was thought to be in danger. On the 10th of
June, however, he played in Le Sicilien before the town.
In the earlier months of 1667 Louis XFV. was \^'ith the
army in Flanders. There were embascies sent from the
comedy to the camp, and on 5th August it was apparent
that Moliere had overcome the royal scruples. Tartuffe
was played, but Lamoignon stopped it after the first night.
Xa Grange and La ToviUicro hastened to the camp, and
got tne king's promise that he would' reconsider the matter
on his return. Moli6re's nest piece (13th January 1668)
was Amphitryon, a free — a very free — adaptation from
Plautus, who then seems to have engaged his attention,
for not long afterwards he again borrowed from the ancient
writer in L'Avare. There is a controversy as to whether
Amphitryon was meant to ridicule M. de Montespan, the
husband of the new mistress of Louis XIV. Michelet has
a kind of romance based on this probably groundless hj-po-
thesis. The king still saw the jjiece occasionally, after he
had purged himself and forsworn sack under Madame de
Maintenon, and probably neither he nor that devout lady
detected any personal references in the coarse and witty
comedy. As usual, Moliere was accused of plagiarizing, this
time from Eotrou, who had also imitated Plautus. The
next play was the inmiortal George Dandin (10th July), first
played at a festival at Versailles. Probably the piece was
a rapid palimpsest on the ground of one of his old farces,
but the addition of these typical members of a coimty
family, the De Sotenville, raises the work from farce to
satiric comedy. The story is borrowed from Boccaccio,
but is of unknown age, and always new, — Adolphus Crosbie
in The Small House at Allington being a kind of modern
■George Dandin. Though the sad fortunes of this peasant
with social ambition do not fail to make us pity him some-
what, it is being too refined to regard George Dandin aa
a comedy with a concealed tragic intention. MoU6re
must have been at work on L'Avare before George Dandin.
appeared, for the new comedy after Plautus was first acted
on 9th September. There is a tradition that the piece
almost failed ; but, if unpopular in the fii'st year of its pro-'
duction, it certainly gained favoiu- before the death of its
author. M. de Pourceavgnac (17th September 1669) was
first acted at Chambord, for the amusement of the king.'
It is a rattling farce. The physicians, as usual, bore the
brunt of Molifere's raillery, some of which is still applicable.
Earlier in 1669 (5th February) Tartuffe was played at
last, with extraordinary success. Les Amants Magnijiques,
a comedy-ballet, was acted first at Saint Germain (10th
February 1670). The king might have been expected to
dance in the ballet, but from Racine's Pritannicus (13th
December 1669) the majestical monarch learned that
Nero was blamed for exhibitions of this kind, and he did
not wish to out^Nero Nero. Astrology this time took the
place of medicine as a butt, but the satire has become
obsolete, except, perhap'i, in Turkey, where astrology is
stiU a power. The Bourgeois Geniilhomme, too familiar
to require analysis, was first played on 23d October 1770.
The lively Fourberies de Scapin " saw the footlights " (if
footlights there were) on 24th May 1671, and on 7th
May we read in La Grange, " les Repetitions de Spsyche
ont commance." La Grange says the theatre was newly
decorated and fitted with machines. A "concert of
twelve violins" was also provided, the company being
resolute to have everything handsome about them. New
singers were introduced, who did not refuse to sing un-
masked on the stage. Quinault composed the words for
the music, which was by LuUi ; Moliere and Pierre Corneille
collaborated in the dialogue of this magnificent opera,
the name of which (Psyche) La Grange eventually learned
how to spell. The Comtesse d'Fscarbagnas (2d February
1672) was anothei piece for the amusement of the courtj.
and made part cf an entertainment called Le Pallet des
Pallets. In this play, a study of provincial manners;
Moliere attacked the financiers of the time in the iJersoD
of M. Harpin. The comedy has little importance compared
with Les Fenunes Savantes (11th February), a severer Pre-
cieuses, in which are satirized the vanity and affectation of
sciolists, pedants, and the women who admire them. The
satire is never out of date, and finds its modern form in;
630
M O L — M O L
Ze Monde oil ton s'eitnitie, by M. Pailleron. ' On the 17th
February Madeleine Bejard died, and was buried at St
Paul. She did not go long befqre her old friend or lover,
Jlolioro. His Manage Force, founded, perhaps, on a
famous anecdote of De Gramont, was played on 8th
July. On 7th August La Grange notes that Moliere was
indisposed, and there was no comedy. Molifere's son died
on the 11th October. On 22d November the preparations
for iha' Malade Imaginaire were begun. On 10th Feb-
ruary 1073 the piece was acted for the first time. What
occurred on 17th Februaiy we translate from the Registre
of La Grange : —
"This same day, about ten o*clock at night, after the comody,
Itonsicur de ilolicre died in his house, Rue.de Richelieu. He had
flayed the part of the said ilalade, suflering much from cold and
inflammation, wliich caused a violent cough. In the violence of
the cough ho burst a vessel in his body, and did not live mora
than half an hour or three-quarters after the bursting of the vessel.
His body is buried at St Joseph's,' parish of St Eustache. There
is a gravestone raised about a foot above the ground."
Mollere's funeral is thus described in a letter, paid
to be by an eye-witness, discovered by M. Benjamin
FiUon :—
"Tuesday, 21st February, about nine in the evening, was buried
Jean Raptiste Poquelin Moliirc, tapissicr valet du cJiambre, and a
famous actor. There was no procession, except three ecclesiastics ;
four priests bore the body in a v.-ooden bier covered with a pall,
six children in blue carried candles iu silver holders, and there
were lackeys with burning torches of wax. The body . , . was
taken to St .Joseph's churchyard, and buried at the foot of the
crosa. There was a great crowd, and some twelve hundred livres
were distr-'buted among the poor. The archbishop had given orders
that Moliere should be interred without any ceremony, and had
even forbidden the clergy of the diocese to do any service for him.
Nevertheless a number of masses were commanded to bo said for
the deceased."
When an attempt was made to exhume the body of
Moliere in 1792, the wrong tomb appears to have been
opened. Unknown is the grave of Moliire.
. Moliere, according to Mile. Poisson, who had seen him
in her extreme youth, was " neither too stout nor too thin,
tall rather than short ; he had a noble carriage, a good leg,
walked slowly, and had a veiy serious expression. His
no.se was thick, his mouth large v/ith thick lips,- his com-
plexion brown, his eyebrows black and strongly marked,
and it was his way of moving these that gave him his comic
expression on the stage." " His eyes seemed to search the
deeps of men's hearts," says the author of ZHmde. The
inventories printed by M. Soulie provo that Moliere was
fond of rich dress, splendid furniture, and old books. The
charm of his conversation is attested by the names of his
friends, who were all .the wits of the age, and the greater
their genius the greitcr their love of Moliere. As an
actor, friends and enemies agreed in recognizing him as
most successful in comedy. His ideas of tragic declamation
were in advance of his time, for he set his face against the
prevalent habit of ranting. His private character was
remarkable for gentleness, probity, generosity, and delicacy,
qualities attested not only by anecdotes but by the evidence
of documents. Ho is probably (as Mcnander is lost) the
greatest of all comic writei-s within tho limits of social and
refined as distinguished from romantic comedy, like that of
Shakespeare, and of political comedy, like that of Aristo-
phanes. He has the humour which is but a sense of the
true value of life, and now takes the form of the most
vivacious wit and the keenest observation, now of melan-
choly, and pity, and wonder at the fortunes of mortal
men. In the literature of France his is the greatest name,
and in the literature of tho modern drama the greatest
after that of Shake^ipeare. Besides his contemplative genius
he possessed an unerring knowledge of the theatre, the
knowledge of a great actor and a great manager, and
hence his plays can never cease to hold tho stasc, and to
charm, if possible, even more in the pcrformaneertlian ia
the reading.
There is no biography of Molicro on a level witli the latest, re-
searches into his lile. The best is probably that of M. Taschereau,
prefixed to an edition of his works (ffiiiwrcs CompUics, Paris, 1363).
To this may bo added 'Jules Loiseleur's'Zi:^ PoiiiiA Obscurs de la
Vie de-MoW.rc, Paris, 1S77. . Wo have seen that iL Loiseleur is
not always accurate, but ho is laborious. "For other books it is
enough to recommend the excellent Bibliographic Moliercsqne of M.
Paul Lacroix (1875), which is an all but faultless guide. The best
edition of Moli^re's works for the purposes of the student is th.'it
published in Lc3 Grands Ecri-nir^ de la France (Hachttte, Parii,
1874-1S82). The edition is still incomplete. It contains reprints
of many contemporary tracts, and. with the Ecgisire of La Grange,
and the Collection iloliircsquc of II. Lacroix, is the chief source of
the facts stated in this notice, in cases where the rarity of docu-
ments has prevented the writer from studying them in the original
texts. Another valuable autliority is the JicchjrcJics sur MoliZrs
ct sur sa Famille of Ed. Soulie (1SS3). Loiheisen's Moliire, seiTi
Lebcn und sciric Wcrlcc (Frankfurt, 1830), is a respectable Ger-
man compilation. Lc Moliiristc (Tresse, Paris, edited by M. Georges
Monval) is a monthly serial, containing notes on Molifere and his
plays, by a number of contributors. The essay;, biographies, plays,
and poems on Moliere are extremely numerous. The best guide to
these is the indispensable Bibliogruphie of M. LacroLx. The English
biographies are few and as a rule absolutely untrustworthy. (A. L. )
MOLINA, Lins (1535-1600), a Spanish Jesuit, whom'
Pascal's Lellres (Tun Provincial have rendered immortal,
was born at Cuenca in 1535. Having at the age of eighteen
become a member of the Company of Jesus, he studied
theology at Coimbra, and afterwards became professor in
the university of Evora, Portugal. From this post he
was called, at the end of twenty )'ear3, to the chair of
moral theology in Madrid, where he died on 12th October
1600. Besides other works he wi-ote Liberi arhitrii cum
graiix donis, divina prxscientia, providentia, prasdesiitiatione
et 7rprobatione, concordia (4to, Lisbon, 15SS); a com-
mentary on tlu5 first part of tho Summa of Thomas Aquinas
(2 vols., fol., Cuenca, 1593); and a treatise De Justitia et
Jure (6 vols., 1593-1609). It is to the first of these that
his fame is principally due. It was an attempt to reconcile,
in words at least, the J^.ugustinian doctrines of predestina-
tion and grace with the Semipelagianism which, as shown
by the recent condemnati6n of Bajus (^r.w.), had become
prevalent in the Roman Catholic Church. A.ssuming that
man is free to perform or not to perform any act v.-hatever,'
Molina maintains that this circumstance renders the gi'aca
of God neither unnecessary nor impossible : — not impossible,'
for God never fails to bestow grace upon those who ask it
with sincerity ; and nat unnecessary, for grace, although
not an efficient, is stiU a sufficient cause of .salvation. Nor,
in Molina's view, does his doctrine of free-will exclude
predestination. The omniscient God, by means of His
" scientia media " (the phrase is Molina's invention, though
the idea is also to be found in his older contempoi-ary
Fouseca), or power, of knowing future contingent events,
foresees how we shall employ our own free-will and treat
His proffered grace, and upon this foreknowledge He can
found His predestinating decrees. These doctrines, although
in harmony with the prevailing feeling of tho Roman
Catholic Church of the period, and further recommended
by their marked opposition to the teachings of Luther and
Calvin, excited violent controversy in some quarters,'
especially on the part of the Dominicans, and at last
rendered it necessary for the pope (Clement VIII.) to
interfere. At first (1594) ho simply enjoined silence on
both parties so far as Spain was concerned ; but ultimately,'
in 159S, ho appointed the "Congregatiode Auxiliis Gratiae"
for the settlement of the dispute, which became more and
more a party one. After holding very numerous sessions,,
tho "congregation" was able to decide nothing, and in
1607 its meetings were suspended by Paul V., win--
announced his intention of himself pronouncing judgmp"t.
in due time. He contented himself, however, in IGll
M 0 L — M 0 L
631
yriih prohibiting all further discussion of the question " de
auxiliis," and studious efforts were made to control the
publication even of commentaries on Aquinas. The
Molinist subsequently passed into the Jansenist controversy,
and it is as a champion of Jansenism that Pascal in the
Provincial Letters attacks Molina and the scientia media
(see Jansenism).
MOLINE, a city of the United States, in Eock Island
county, Illinois, is situated in a picturesque district on the
left bank of the Mississippi, opposite the upper end of Rock
Island. First settled in 1832, the town was organized as
a city in 1872. It is noted for its water-power, developed
and maintained by the Government, and for the number and
importance of its manufacturing establishments. By means
of a dam nearly a mile in length, from the Illinois shore
to the island, an almost uniform head of 7 feet of water is
obtained, which is used in driving the machinery of the
Government arsenal on the island, and in supplying power
to several factories. Beds of bituminous coal are mined in
the neighbourhood, and three lines of railway pass through
the city, affording with the river ample means of communi-
cation. The most prominent manufactures are agricultural
implements and machinery generally, waggons, organs,
paper, and stoves. Moline has nine churches, a complete
system of graded free schools, including a high school, and
a free library. The population increased from 40C6 in
il870 to 7805 in 1880, and with the siiburbs the number
is now estimated at 12,000.
MOLINOS, Miguel de (1627 -c. 1696), a Spanish
•priest whose name is intimately associated with that type
of religion known in Italy and Spain during the latter
half of the 17th century as Quietism, was born of good
family in the diocese of Saragossa, on 21st December 1627.
Having entered the priesthood, he settled about his fortieth
year in Rome, where he speedily rose to high repute as a
father confessor, and gained many distinguished friends,
among whom were several cardinals, including Odescalchi
(afterwards Innocent XI., 1676). In 1675 he published jft
Rome a small duodecimo volume entitled Guida spiriluale
che disinvolr/e. I'anima e la conduce per I'interior camino all'
acquisto delta perfella contemplazione e del ricco tcsoro deila
pace interiore, wliich was soon afterwards followed by the
Breve trattato della cottidiana commtmione, usually bound
up with it in later editions. The work, which breathes a
spirit of simple and earnest piety, is designed to show how
inward peace may be found by what may be called con-
templative or passive prayer, by obedience, by frequent
communion, and by inward mortification ; it was widely
circulated, and greatly increased the popidarity of its
author, whom Innocent XI. after his elevation provided
(•with rooms in the Vatican, and is said to have also taken
as his spiritual director. Its doctrine of the passivity of
the highest contemplation and purest prayer does not
appear to have raised the slightest discussion until after
the publication, in 1681, of the Concordia ira la fatica e
la tjmele nelV oratione, by the Jesuit preacher, Paolo Scgneri.
■Although scrupulously refraining from any mention of
the name of Molinos, and indeed displaying considerable
moderation as a controversialist, Segneri by this tract and
by another with which he followed it up brought upon
himself much unpopularity; and so great did the excitement
become that a committee was at last appointed by the
Inquisition to investigate his own views as well as to
examine the writings of Molinos'and of his friend Petrucci
1 author of La contemplazione mistica acquistata). The
.t:port (1682) was entirely favourable to the doctrines of the
\Juid<j Spirit-uale, the writings of Segneri being censured
»s icandalous and heretical; but in 1685, in consequence
ot rfinresentations made to the pope by Louis XIV., under
«Sa tfesmf influence of Pcrc La Chaise, botli Petrucci and
Molinos -were laid under arrest, and the 2>apers of the latter,
including a voluminous correspondence, seized. Pelnicci
was soon afterwards liberated, and relieved from further
persecution by the gift of a cardinal's hat ; but, after Molinos
had languished in confinement for two years, suddenly 200
persons, many of them of high rank, were also apprehended
by order of the Inquisition for what were then for the first
time called " Quietist" opinions. In 1687 the pope signi-
fied his ajjproval of the condemnation pronounced by the
Inquisition on sixty-eight doctrines imputed to Molinos.
The "heretic" forthwith " abjured " these, and tlius escaped
the flames indeed, but did not regain his liberty. Of liis
later years nothing is known ; according to the most prob-
able accounts he languished in imprisonment imtil 28th
December 1696.
The evidence on which certain charges of immoralitj' against
Ilolinoa were based is unknown, and the degree of his responsibility
for certain of the condemned propositions is obscure; but a penisalof
the Guida Spiriluale at least docs not disclose to the candid rea<icr
any reason whcrelbre Jloliiios should not have been tolerat,-;d within
a church which has canonized St Theresa. The expknation of tho
treatment to which he was subjected is most probably to be souglit
rather in the negative than in the positive .ispects of l>is teaching,
and still more in tho passing exigencies of party politics. As
Tholuck remarks, it was liardly to be expected that the Society of
Jesus should regard as otherwise than highly dangerous a man who
"declared confession and outward mortification to bo work only
for beginners, who himself abstained from confessing for tu'clve'
j'cars on end, by whose advice countless monks and nuns had'
thrown aside chaplets, images, and reliqnes, that they might
worship God in the spirit, and who, moreover, stood well with
tho fashionable world and with tho pope himself." Tho Guida
Spiriluale w.t3 published in Spanish at Madrid in 1676, and fre-
quently aftenvards ; it was also translated into Latin {Ma.midv.clio
Hjiirilvalis, Leipsic, 1687) by A. H. Francko, tho well-known
German pietist and philanthropist, and an English version (The
spiritual guide, which discnlanylcs the sotil and brimjs it hy the
inward way to tlic getting of perfect contemplation and the rich
treasure of eternal peace ; with a brief treatise concerning daily
enmmunion) appeared in 1688. Tho materials for a history of
the Quietist controverey are very fully given in the third volumo
of Gottfried Arnold's KircJicn-und Kctzcrhistorie. See also Heppe,
Ocschiehte der guictistischcn Mi/stik in der . Katholischcn Kircha
(Berlin, 1875) ; Tholuck's article on " jMolinos " in Herzog's
Jlealcncyklopadie ; and Bigelow, Molinos the Quietist, New York,
1882.
ilOLISE, now Campobasso, a province of Italy, stretch-
ing twenty miles along the coast of the Adriatic, and
bounded by the Abruzzi (Chieti and Aquila), Terra di
Lavoro (Caserta), Benevento, and Capitanata (Foggia).
Most of it lies on the north-eastern side of the Apennines,
and is watered by the Biferno, the Forlone, and the Trigno ;
but it also includes the country on tho other side which
contains the head streams of the Volturno. About five-
sixths of the surface may be described as mountainous or
hilly, the loftiest range being the Matese on the borders
towards Benevento, with its highest point in Jlonte
Jliletto, 6750 feet. Tho population, which increased from
346,007 in ISGl to 365,434 in ISSl, is mainly dependent
on pastoral and agricultural piu^suits, neither manufactures
nor trade being highly developed. According to the census
of 1871, there were six places with more than 5000 inliabit-
ants— Campobasso, 12,890; Riccia, 8123; Isernia, 7715;
Agnone,7147; Cascalende,6217; and Larino, 5357; accord-
ing to the census of 1881, 21 of the 133 communes had a
population exceeding 4000.
The Molise territory was in ancient times part of Iho country of
the Sabines and Pamnites. Under the Lombards it was included
in the duchy of Benevento; but the districts of Scpino, Boiano*
and Iscmia were cut off to form a domain for tlio liulgaiians who had
come to assist King Grimoald. About two centuries later tliis became
the countship of Boiano, and tho name was soon after changed to
countshii)of Molise, probably because the lordship w.is held byUgono
di Molisio, or Molise. Attached under Frederick H. to tho Terra di
Livoro, and at a later date ineoi-porated with Capitanata, tho district
did not again become an independent province till 1811. In 1861
it sun'cndcred fifteen communes to Benevento, and received thirteen
from Terra di Lavoro. '
632
MOLLUSCA
THE Mollusca form one of the great " phyla," or sub-
kingdoms of the Animal Pedigree or Ivingdom.
Liteyary Hidoi^ of the Group. — The shell-bearing forms
belonging to this group which were known to Linnaeus were
placed by him (in 1748) in the third order of his class
Vermes under the name " Testacea," whih:t tlia Echino-
derms, Hydroids,_and Annelids, with the naked Molluscs,
formed his second order, termed " Zoophyta." Ten years
later he replaced the name "Zoophyta" by "Mollusca,"
which was thus in the first instance applied, not to the
Mollusca at present so termed, but to a group consisting
chiefly of other organisms. Gradually, however, the term
Mollusca became used to include those Jlollusca formerly
placed among the "Testacea," as well as the naked iioUusca.
It is important to observe that the term jiaXiKia, of which
Mollusca is merely a Latinized form, was used by Aristotle
to indicate a group consisting of the Cuttle-fishes only.
The definite erection of the Mollusca into the position
of one of the great primary groups of the animal kingdom
is due to George Cuvier (1788-1800), who largely occupied
himself with the dissection of representatives of this type (1).'
An independent anatomical investigation of the MoUusca
had been carried on by the remarkable Neapolitan natur-
alist Poll (1791), whose researches (2) were not published
until after liis death (1817), and were followed by the
beautiful works of another Neapolitan zoologist, the illus-
trious Delle Chiaje (3).
The " cmbranchement " or sub-kingdom Mollusca, as de-
fined by Cuvier, included the following classes of shell-fish :—
1 , the cuttles or poulps, under the name Cephalopoda ; 2,
the snails, whelks, and slugs, both terrestrial and marine,
under the name Gastropoda ; 3, the sea-butterflies or
winged-snails, under the name Ptekopoda ; 4, the clams,
mussels, and oysters, under the name Acephala ; 5, the
lamp-shells, under the name Bp.achiopoda ; 6, the sea-
squirts or ascidians, under the name Nuba ; and 7, the
barnacles and sea-acorns, under the name Cikrhopoda.
The main limitations of the sub-kingdom or phylum
Mollusca, as laid do^vn by Cuvier, and the chief divisions
thus recognized ivithin its limits by him, hold good to the
present day. At the same time, throe of the classes con-
sidered by him as Mollusca have been one by one removed
from that association in consequence of improved know-
ledge, and one additional class, incorporated since his day
with the Mollusca ■with general approval, has, after more
than forty years, been again detached and assigned an
independent position owing to newly-acquired knowledge.
The first of Cuvier's classes to be removed from the Iifol-
lusca was that of the Cirrhopoda. Their aflinities with the
lower Crastacea were recognized by Cuvier and his contem-
poraries, but it was one of the brilliant discoveries of that
remarkable and too-!ittle-honoured naturalist, J. Vaughan
Thompson of Cork, which decided their position as Crus-
tacea. The metamorphoses of the Cirrhopoda were described
and figured by him in 1830 in a very complete manner,
and the legitimate conclusion as to their affinities was for-
mulated by him (4). Thus it is to Thompson (1630), and
not to Burmeister (1831), as erroneously stated by Kefer-
stoin, that the merit of this discovery belongs. The i.ext
class to bo removed from Cuvier's Mollusca was that of the
Nuda, better known as Tunicata. In 1SG8 the Russian
embryologist Kowalewsky startled the zoological world with
a minute account of the developmental changes of Ascidia,
one of the Tunicata (5), and it became evident that the
' Theso ngur&i refer to the biblic
. C9o.
;r.)i'hy ai Iho enil of tha article.
afiinities of that class were with tha Yerlebrata, whilst their
structural agreements with MoUusci were only superficial.
The last class which has been removed from the Cuvierian
Mollusca is that of the Lamji-shells or Brachiopoda. The
history of its dissociation is connected with that of tha
class, viz., the Polyzoa or Bryozoa, which has been both
added to and again removed from the MoUusca between
Cuvier's date and the present day. The name of J.
Vaughan Thompson is again that which is primarily con-
nected with the history of a Molluscan class. In 1830
he pointed out that among the numerous kinds of " polyps"
at that time associated by naturalists with the Hydroids,
there were many which had a pecuhar and more elaborate
type of organimtion, and for these he proposed the name
Polyzoa (6). Subsequently (7) they were termed Bryozoa
by Khrenberg (1831).
Henri Milne-Edwards in 18-14 demonstrated (8) the affi-
nities of the Polyzoa with the Molluscan class Brachiopoda,
and proposed to associate the three classes Brachiopoda,
Polyzoa, and Tunicata in a largo group " MoUuscoidea,".
coordinate with the remaining classes of Cuvier's ilollusca,
which formed a group retaining the name Mollusca. By,
subsequent -(vriters the Polyzoa have in some cases been kept
opart from the !Mollusca and classed with the " Vermes ; "
v/hilst by others (including the present writer) they have,
together with the Brachiopoda, licen regarded as time Mol-
lusca. The recent investigation by Mr. Caldwell (1882)
of the developmental history of Phoronis (9), together
with other increase of knowled'.'e, has now, however, estab-
lished the conclusion that the agreement of structure
su)->posed to'obtain between Polyzoa and true Mollusca is
delusive; and accordingly they, together with the Brachi-
opoda, have to be removed from the Molluscan iihyluni.
Furtlier details in regard to this, the last revolution in Mol-
luscan classification, will be fouud in the article Polyzoa.
As thus finally purified by successive advances of era-
brj'ological research, the JloUusca are reduced to tho
Cuvierian classes of Cephalopoda, Pteropoda, Gastropoda,
and Acephala. Certain modifications in the disposition of
these classes are naturally enough rendered necessary by,
the vast accumulation of knowledge as to the anatomy and
embryology of the forms comprised in them during fifty
years. Foremost amongst those who have within that
period laboured in this gi-oup are the French zoologists
Henri Milne-Edwards (20) and Lacaze Duthiers (81), to
the latter of whom we owe the most accurate dissections
and beautiful illustrations of a number of different types.
To KoUiker (23), G egenbaiu: (23), and more recently Sjjengel
(24), amongst German anatomists, wo are indebtod for
epoch-making researches of the same kind. In England,
Owen's anatomy of the Pearly Nautilus (10), Hu.xley's dis-
cussion of the general morphology of the Mollusca (11),
and Lanko.'^ter's erabryological investigations (13), Iiare
aided in advancing our knowledge of the gi'oup. Two
remarkable works of a systematic character dealing with
the JloUusca deserve mention here — the Manual of ihe^
Mollusca by the late Dr. S. P. Woodward, a model of clear,
systematic exposition, and the cjdiaustive treatise on tha
Malacozoa or Wcichthiere by the late Professor Kefcrstein,
of Giittingen, publislied as part of Broun's Classen und
Ordiimirten des Thicr-Jieic/is. The latter work is the most
completely illustrated and most exhaustive survey of exist-
ing knowledge of a large division of the animal kirgdom
whi( h has ever been produced, and, whilst forming a monu-
ment to its lamented author, places the student of Mol-.
lusciin morpliology in a peculiarly favourable prsition.
M O L L U S G A
633
Claigea of the Mollusca. — The classes of the Jlollusoa
which we recognue are as folli-sre : —
Phylum MoLLtracA.
Branch A. — Glossophora.
Beanoh B.— Lipoccphala
( = Acephala, Cuvitr).
Class 1. — Lamellibranchia
(Syn. Conchifera).
£camjt>;o-— Oyster, Mussel,
Clam, Cocl^le.
Class 1. — Gastropoda.
Br. a. — Isoplcura.
Examples — Chiton, Neo-
inenia.
Br. b. — AnisopUnra,
Examples — Limpet, 'VVhelk,
Snaii, Slug.
Class 2. — SCAIUOPODA.
Examine— T:<MXlisae\!L
Class 3. — Ckphalopooa.
Br. a. — PUropoila.
Examples — Hyalaea, Pnea-
modermon.
Br. b. — Siphonopnda.
Examples — Kautiluai Cut-
tles, Poulp.
General CItaracters of the Mollusca. — The forms com-
prised in the above groups, whilst exhibiting an extreme
range of variety in shape, as may be seen on comparing
an Oyster, a Cuttle-fish, and a Sea-slug such as Doris ;
whilst adapted, some to life on dry land, others to the
depths of the sea, others to rushing streams ; whilst capable,
some of swimming, others of burrowing, crawling, or jump-
ing, some, on the other hand, fixed and immobile ; some
amongst the most formidable of carnivores, others feed-
ing on vegetable mud, or on the minutest of microscopic
organisms — yet all agree in possessing in common a very
considerable number of structural details which are not
possessed in common by any other animals.
The structural features which the Mollusca do possess
in common with other animals belonging to other great
phyla of the animal kingdom are those characteristic of
the Ccelomata, one of the two great grades (the other and
lower being that of tha Ccelentera) into which the higher
animals, or Enterozoa as distinguished from the Protozoa,
are divided (13). The Enterozoa all commence their indivi-
dual existence as a single cell or plastid, which multiplies
itself by transverse division. Unlike the cells oi the Proto-
zoa, these embryonic cells of the Enterozoa do not remain each
like its neighbour and capable of independent life, but pro-
ceed to arrange themselves in two layers, taking the form
of a sac. The cavity of the two-cell-layered sac or Diblas-
tula thus formed is the primitive gut or akch-enteron.
In the Coelentera, whatever subsequent changes of shape
the little sac may undergo as it grows up to be Polyp or
Jelly-fish, the original arch-enteron remains as the one
cavity pervading all regions of the body. In the Ccelomata
the arch-enteron becomes in the course of development
divided into two totally distinct cavities shut off from one
another — an axial cavity, the ilet-e-steeon, which retains
the fimction of a digestive gut ; and a peri-axial cavity,
the CCELOM or body-cavity, which is essentially the blood-
space, and receives the nutritive products of digestion and
the waste products of tissue-change by osmosis. The
Mollusca agree in being Cffilomate with the phyla Verte-
hrata, Platyhelmia (Flat-worms), Echinoderraa, Appendicu-
lata (Insects, Ringed-worms, ic), and others, — in fact,
with all the Enterozoa except the Sponges, Corak, Pol>-ps,
and Medusa.
In common with all other Ccelomata, the Mollusca
are at one period of life possessed of a pkostoxiium
or region in front of the mouth, which is the essential
portion of the "head," and is connected with the property
of forward locomotion in a definite direction and the steady
carria<,e of the body (as opposed to rotation of the bouy
on its long axis). As a result, the Ccelomata, and with
them the MouiL<<-a pres,6i,t (in the first instance) the general
16—23*
couditicji of body known ;is BrL.'.Ti;r.AX. esmmstky; the
dorsal is differentiated from the ventral surface, whibt a
right and a left side similar to, or rather the comp'emenJ.s
of, one another are permanently established. In common
with aU other Ccelomata, the Mollusca have the mouth and
first part of the aUinontory canal which leads into the
met-enteron formed by a special invagination of the outer
leyer of the primitive body-wall, not to be confounded with
that which often, but not always, accompanies the ante-
cedent formation of the arch-enteron ; this invagination
is termed the ST0M0D.i:crsr. Similarly, an anal aperture is
formed in connexion with a special invagination which
meets the hinder 'part of the met-enteron, and ia termed
the PB0CT0D.EtTir.
In common with many (if not all) Coslomata, the Mol-
lusca are provided with at least one pair of tube-like organs,
which open each by one end into the coelom or body c.vity,
and by the other end to the exterior, usually in t.'ie neigh-
bourhood of the anus. These are the nepheidu
Like all other Ccelomata, the Mollusca are also p'lvided
with enocint groups of cells forming usually paired or mediart
growths upon the walls of the ccelomic cavity, the cells
being spe- ially pos.-,Li3ed of reproductive power, ind dif-
ferentiated as egg-celis and sperm-cells. These are the
gonads. As in other Ccelomata, the cells of the jjonads
may escape to the exterior in one of two ways — either
through the nex'hridia, or, on the other hand, by special
apertures.
As in all other Coelomat^^ the cells, which build np
respectively the primary outer layer of the body, the
lining l«yer of the met-enteron, and the hning layer of the
coelom, are multiplied and differentiated in a variety ofi
ways in the course of growth from the early embryoiiio
condition. Tissues are formed by the adhesion of a num-<
bet of similarly modified cells in definite tracts. As in all
Ccelomata, there is a considerable variety of tissues char^
acterized by, and differentiated in relation to, particular
physiological activities of the organism. Not only the
Ccelomata but also many Ccelentera show, in addition to
the EPITHELIA (the name given to tissue which bounds a
free surface, whether it be that of the outer body-wall, of
the gut, or of a blood-space), also deeper lying tissues,
of which the first to appear is iiusculab tissue, and tha
second xervous tissue.
The epithelia aie active in throwing off their constituent
cells (blood-corpuscles from the wail of the coelom), or in
producing secretions (glands of body-wall and of gut), or
in forming horny or calcareous plates, spines, and pro-
cesses, known as cnriccLAK proditcts (shells and bristlea
of the body-wall, teeth of the tongue, gizzard, &c.).
In the ilollusca, as in all other Ccelomata, in correspond-
ence with the primary bilateral symmetry ana lu relation
to the special mechanical conditions of the prostomium,
the nervous tissue which is in Coelentera, and even in Flat^
worms, diffused over the whole body in networks, tends
to concentrate in paired lateral tracts, having a special
eula.-gement in the prostomium. The earlier plexifomi
arrangement is retained in the nervous tissue of the walls
of the alimentary canal of many Ccelomata, whilst a con-
centration to form large nerve-masses (oa>'GLIa), to which
numerous afferent and efferent fibres are attached, affects
the nervous ti.ssue of the body-wall.
In all Ccelomata, including Mollusca, muscular tisme is
developed in two chief layers, one subjacent to the dcric or
outer epithelium (somatic MCscutATtJRE), and a second sur-
rounding the alimentary canal (spi,a>xhnic MCscaLATtTRE).
Thus, primarily, in Ccelomata the body has the character of
two muicular sacs or tubes, placed one ■nifhin the other
and separated from one another by the ca-lomic space.
The somatic musctilature is the more cojiious and develops
G34
M 0 L L U S C A
[schematic MOIXTJSa'
very generally an outer circular layer (i.e., a layer in which
the muscular fibres run in a di'-'^ction transverse to the
lenj; axis of the body) and a deeper longitudinal layer ;
to these oblique and radiating fibres may be added. The
splanchnic musculature, though more delicate, exhibits a
circular layer nearer the enteric epithelium, and a longi-
tudinal layer nearer the coslomic surface.
In Coclomata and in many Coclentera there arc found
distributed between the tracts of muscular tissue, bounding
them and giving strength and consistency also to the walls
of the body, of the alimentary canal, of the ccelom, and of
the various organs and tissue-masses (such as nerve-centres,
gonads, itc.) concocted with these, tracts of tissue the
function of which is skeletal. The skeletal tjssite of
MoUusca, in common with that of other Ccelomata, exhibits
a wide range of minute structure, and is of differing density
in various parts ; it may be fibrous, membranous, or carti-
laginous. The Hollusca, in common v-ith the other Ccelo-
mata, exhibit a rcniarl;able kind of association between the
various forms of skeletal tissue and the epithelium which
lines the coelom.ic cavity. Tlie ccelomie cavity contains a
liquid which is albuminous in chemical composition (blood-
lymph or h.emolymph), apd into this liquid cells are shed
from the coelomic epithelium. They float therein and are
known as blood corpuscles or l\"MPH corpuscles. The
coslomic space with its contained hiemolymph is not usually
in Ccelomata, and is not in MoUusca, a simple even-walled
cavity, but is broken up into numerous passages and re-
cesses by the outgro'wths, both of the alimentary canal and
of its own walls. By the adhesion of its opposite walls,
and by an irregularity in the process of increase of its area
during growth, the ccelom becomes to a very large extent a
spongy system of intercommunicatiug LACUN.B or irregular
spaces, filled with the coelomic fluid. At the same time, the
coelomic space has a tendency to push its way in tlic form of
narrow canalsand sinuses between the layersof skeletal tisaue,
and thus to permeate together with the skeletal tissue in
tlie form of a spongy, or it may be a tubular, network all
the apparently solid portions of the animal body. This
association of the nutritive and skeletal functions is accom-
panied by a complete identity of the tissues concerned in
these functions. Not only is there complete gradation
from one variety of skeletal tissue to another (e.g., from
membranous to fibrous, and from fibrous to cartilaginous)
even in respect of the form of the cells and their intercellular
substance, but the cffilomic epithelium, and consequently
the haimolj'mph with its floating corpuscles derived from
that ei)ithelium, is brought into the same continuity. The
skeletal and blood-containing and -producing tissues in fact
form one widely-varying but continuous whole, which may
be called the skeleto-trophio system of tissues.
In many Cffilomata not only do the skeletal tissues
allow the coelomic space with its fluid and corpuscles to
penetrate between their layers, but a special mode of
extension of that space is found, which consists in the
liollowng out of the solid substance of elongated cells
liaving tlie form of fibres, which thus become tubular,
and, admitting the nutritive fluid, serve as channels for
its distribution. These are " capillary vessels," and it has
yet to be shown that such are formed in the MoUusca.
Larger vessels, however, concerned in guiding the move-
ment of the coelonuc fluid in special directions are very
usually developed in the MoUusca, as in other CcEloma,ta,
by the growth of skeletal tissue around what are at first
ill-defined extensions of the ccelomie space. In this way
a, portion of the coelomic space becomes converted into
vessels, whilst a large part remains with irregular walls
extending in every direction between the skeletal tissues
and freely communicating with the system of vessels. As
•injnany other Ccelomata, mascular tissuo grows around
ths hrgest vessel formed from the primitive coelom, which
thus becomes a contractile organ for projjelling the blood-
lymph fluid. This " he.\p.t " has in llollusca, as in most
other Coolomata in which it is developed, a dorsal position.
A communication of the blood-lymph space with the
exterior by means of a pore situated in the foot or else-
where has been very generally asserted to be characteristic
of MoUusca. It has Deen maintained that water is intro-
duced by such a pore into the blood, or admitted into a
special series of water-vessels. It has also been asserted
that the blood-fluid is expelled by the JloUusca from these
same pores. Recent investigation (14) has, however, made
it probable that the pores are the pores of secreting glands,
and do not lead into the vascular system. There is, it there-
fore appears, no admission or expulsion of water through
such pores in connexion with the blood, although in some
other Crelomata it is established that water is taken into
the ccelomie space through a pore (Echinoderms), whilst in
some others there is no doubt that the ccelornic htemoljTnph
is occasionally discharged in quantity through pores of defi-
nite size and character (Earthworm, &c.).
We have thus seen that the MoUusca possess, in common
with the other Ccelomata — 1, a body composed o^a vast
number of ce/ls or plastids, arranged so as to form a sac-
like hody-wall, and within that a second sac, the met-enteron,
the wall of which is separated from the first by a coslom or
blood-lymph space ; 2, a slomrA-mmi and a proctodawm ;
3, a prostomium, together with a differentiated dorsal and
ventrcd sarface, and consequently right and left sides, i.e.,
bilateral symmetry ; 4, a pair of nephridia ; 5, gonads
developed on the wall of the coelom ; 6, deric epithelium
(producing horny and calcareous deposits on its surface),
enteric epithelium, and cielomic epithelium ; 7, laterally
paired masses of nerre-tissiie, especially large in the pro-
stomial region (nerve-centres or ganglia) ; 8, muscular
tissue, forming a somatic tunic and a splanchiic tunic ; 0,
skeleto-trophic tissues, consisting of membranous, fibrous, and
cartilaginous supporting tissues, and of blood-vessels and the
walls of blood-spaces, the coelurnic eplt/icliuin, and the liquid
tissue known as hxmolympk (commonly blood).
'Schematic Mollusc. — Starting from this basis of stractural
features common to them and the rest of the Cffilomata,
we may now point out A\hat are the peculiar developments
of structure which characterize the MoUusca and lead to
the inference tho^ they are members of one peculiar branch
or phylum of the animal pedigree. In attempting thus to
set forth the dominating structural attributes of a great
group of organisms it is not possible to make use of arbi-
trary definitions. Of JloUusca, as of other great phyla, it
is not possible categorically to enunciate a series of struc-
tural peculiarities which will be found to be true in refer-
ence to every member of the group. We have to remember
that the process of adaptation in the course of long ages
of de\'elopment has removed in some cases one, in other
cases another, of the original features characteristic of the
ancestors from which the whole group may be supposed to
have taken origin, and that it is possible (and' actually is
realized in fact) that some organisms may have lost all the
primary characteristics of MoUuscan organization, and yet
be beyond all doubt definitely stamped as MoUusca by
the retention of some secondary characteristic which is so
peculiar as to prove their relationsliip v.'itli other MoUusca.
An example in point is found in the curious fish-like form
Phyllirhoe (fig. 5t>), which has none of the primaiy char-
acteristics of a Mollusc, aiid yet is indisputably proved to
belong to the MoUuscan phylum by possesf ing the peculiar
and elaborate lingual apjiaratus present in one branch of
the phylum, the Glossophora.
In order to exhibit concisely the jicculiarities of organi-'
zation which characterize the MoUasc.a, we find it moa,
SCHEilATlC mollusc]
convenient, to construct a schematic Mollusc, -which shall
possess in arj unexaggerattd form the various structural
arrangements which are more or less specialized, exagger-
ated, or even suppressed in particular members of the group.
Such a schematic Mollusc is not to be regarded aa an arche-
M 0 L L U ^ U xi.
635
rio. I.— Schemr.flc Mollusc. A. Dorsal aspect B. Ventral aspect C. The
beai-t, pericardium, gonads, and nepltridia shown in positiob. D. The nervous
system ; the reader is requested to note that the cord passing backwards
from y,ve lies beneath- ani does not in any way unite with tlie cord which
Jiasses irom g.ab to g.pt. E. Diaj^m in which the body-wall is represented
Its (;ut ID the median antero-posterior plane, so as to show oreads in position,
— the shell-sac is seen in section, but the shell is omitted.
Letters In all the figures as foIIOAvs : — a, cephalic tentacle ; fc, head ; c, edge
of the mantle-skirt or linibus pallialis; d, dotted line indicating the line or
origin of the free mantle-skii-t Iroin the sides of the visceral hump ; e, outline
of tlie foot seen through tlie mantle-skirt in A, which is supposed to be trans-
prent, allowing the position of this and of the various parts ;i, (, h, ^ m, to
be seen through its substance ; /, edge of the shell-follicle ; p, the shell ; A,
the osphradium, paired (.Spengel's olfactory organ) ; f, the ctenidiuin, paired
<giU-pluine) ; fc, aperture of the gonad, paired ; t, aperture of one of the two
Dephridia ; m, anus ; n, posterior region of the foot reaching farther back
than the mass of viscera (dorsal hump) which it carries ; o, mouth ; p, plantar
SQrface of the foot ; <j, cut edge of the body-wall of the dorsal region ; r,
cceloniic space Cblood-lymph space or body-cavity), mostly occupied by liver,
but to some extent retained as blood-channels aud lacuniB; «, pericardial
cavity ; (, gonad (ovary or spermary), paired ; «, nephridium, paired ; r, ven-
tiiclo of the he.irt receiving the right and the left auricles at its sides, and
sending off anteriorly a large vessel, posteriorly a small one ; w, the cephalic
eye, paired ; z, dotted ring to show the position occupied by the esophagus
In relation to the ner^■e ganglia and cords : y, the otocyst, paired : e.t, the
digestive eland (so-called " liver") of the left side ; s.i, duct of the digestive
gland of the riglit side ; g.e, cerebral ganglion united by the cerebnu com-
missure to its fellow : j7.p/, pleural ganglion united by the cerebro-pleural
connective to the cerebral ganglion, and by the pleuro.pedal connective to
the pedal ganglion ; g.pe, the pedal ganglion united to its fellow by the pedal
coniniissunj— the two sending off posteriorly the long laddcr.like pair of pedal
nen-cs ; ff.v, the visceral ganglion (of the left side) united by tlie visceral
loop or commissure to the similar ganglion, on the right side, and by tlie
visccro-pleural connective to the pleiu-al ganglion ; g.ab, abdominal ganglion
developed on the course of the visceral loop ; g.olf, olfactory ganglion placed
near the osphradium on a nerve taking its origin from the visceral ganglion.
type, in the sense which has been attributed to that word,
nor as the embodiment of an idea present to a creating mind,
nor even as an epitome of developmental laws. Were know-
ledge sufficient, wo should wish to make this schematic
Mollusc the representation of the actual jrolluscan ancestor
from which the various living forms have sprung. To defi-
nitely claim for our schematic form any such significance
in the present state of knowledge would be premature,
but it may be taken as more or l^-ss coinciding v.ith what
we are justiiied, under present conditions, in picturing to
ourselves as the original Mollusc or archi-MoUusc (more
correctly Archimalakion). After describing this schematic
form, we shall proceed to show how far it is realized or
justified in each class and order of MoUusca successively. ■
The schematic Mollusc (fig. 1, A to E) is oblong in
shape, bilaterally symmetrical, with strongly differentiated
dorsal and ventral surface, and has a v/ell-marked head,)
consisting of the prostomium (6) and the region immeJ
diately behind the mouth. Upon the head we place a!
pair of short cephalic tentacles (a). The mouth is
placed in the median Uno anteriorly, and is overhung by
the prostomium (B, o) ; the anus is placed in the median
lino posteriorly, well raised on the dorsal surface (A, m)i
The apertures of a pair of nepkridia are seen in tha
neighbourhood of the anus right and left (A, I). Neai
the nephridial aperttues, and in front of them, right an4
left, are the pair of apertures (k) appropriate to the ductd
of the GONADs^(generative pores).
The most permanent and distinctive MoUuscan organ
is the FOOT (Podium). This is formed by an excessive
development of the somatic musculature along the ventral
surface, distinctly ceasing at the region of the head, below
which it suddenly projects as a powerful muscular piass
(B, p ; E, p). It may be compared, and is probably genetic-
ally identical, wth the muscular ventral surface of the
Planarians and with the suckers of Trematoda, but is more
extensively developed than are those corresponding struc-
tures. The muscular tissue of the foot, and of all other
parts of the body of all Mollusca, is cellular and unstriated,
as distinguished from the composite muscular fibre (con-
sisting of cell-fusions instead of separable cells) which
occurs in Arthropoda and in Vertebrata, and which has
the, further distinction of being composed of alternating
bands of substance of diflering refractive power (hence
"striated"). The appearance of cross striation seen in
the muscular cells of some Molluscs (odontophore of
Haliotis, Patella, <tc.) requires further investigation. It
is by no means altogether the same thing as the mark-
ing characteristic of striated muscular fibre.
Contiasting with the ventral foot is the thin-walled
dorsal region of the body, which may be termed the antr-|
podial region. This thin-walled region is formed by softi
viscera covered in by the comparatively delicate and non-
muscular body- wall (fig. 1, E). As the ventral foot is.'
clearly separate from the projecting head, so is this dorsalj
region, and it is conveniently spoken of as the viscekalJ
HtTMP or " dome " (cupola). Protecting the visceral dome
is a SHELL (conchylium) consisting of a homy basis impreg-j
nated with carbonate of lime,' and secreted by the deric
epithelium of this region of the body (<?). The shell
in oui- schematic Mollusc is single, cap-shaped, and sym-
metrical. It does not lie entirely naked upon the surface
of the visceral dome, but is embedded all round its margin,'
to a large extent in the body-wall. In fact, the integu-
ment of the visceral dome forms an open flattened sac
in which the shell lies. This is the pehiaky shell-
sac, or follicle (A and E, /). The wall of the body pro-'
jects all round the visceral dome in the form of a flap or,
skirt, so as to overhang and conceal to some extent the'
head and the sides of the foot. This skirt, really an out-j
' As to the minute structure of the sliell
Carpenter's article " Shell " in the Cyclop, of A
limits of our space do not permit
logical topics.
vaiious classes, seo
(. <tnd PInisiol. Th»'
to dcaJ with this or other Lisioi
63(i
M O L L U S C A
[schematic mollusc.
growtn of the dorsal body-wall, is called the mantle-plap
ilimbus palUalis), or more shortly the mantle or pallium;
c). The space between the overhanging mantle-flap and the
tides and neck of the animal which it overhangs is called
the stTC-PALLLU. SPACE Of CHAMBEE. Posteriorly in this
space are placed the anus and the pair of nephiidial aper-
tui'es (see Cg. 1, E).
The development of the mantle-skirt and Its sub-pallial
space appears to have a causal relation, in the v.-ay of pro-
tection, to a pab of processes of the body-wall vrhich
spring, one on the right and one on the left, from the sides
of the body, nearer the anus than the mouth, and jre
concealed by the mantle-flap to some extent (A, B, i).
These processes have an axis in which are two blood-vessels,
and are beset v.ith two rows of flattened filaments, like the
teeth of a comb in double series. These are the ctenidia
or gill-combs. Usually, as v/L!l be seen in the sequel, they
play the part of gills, but since in many lIoUuscs (Lamelli-
branchs) theu: function is not mainly respiratory, and since
also other completely-formed gills are developed as special
organs in some Molluscs to the exclusion of these pro-
cesses, it is well not to speak of them simply as " gills " or
"branchiie," but to give them a non-physiological name
such as that here proposed. Near the base of the stem of
each ctenidium is a patch of the epithelium of the body-
wall, peculiarly modified and supplied with a special nerve
and ganglion. This is Spengel's olfactory organ, which
tests the respiratory fluid, and is persistent in its position
and nerve -supply throughout the group MoUusca. We
propose to call it the ospheadium.
Passing now to the internal organs, our schematic
Mollusc is found to possess an alimentaky cvnal, which
passes from mouth to anus in the middle line, leaving
between it and the muscular body-wall a more or less
spongy, in parts a spacious, coslom. The stomodeeum is
large and muscular, the proctodicum short ; the bulk of
the alimentary canal is therefore developed from the met-
enteron or remnant of the arch-enteron after the coelom
has been pinched off from it. A paired outgrowth of the
met-enteron forms the glandular diverticulum knovra as
the digestive gland or (co:nmcn!y) liver (E, !ff, :l).
Dorsally to the alimentary tract the cixlom is spacious.
The space (C, E, s) is termed the PEracARDimi, since it is
traversed by a vessel running fore and aft in the median
line, which has contractile muscular walls and serves as a
heart to propel the ccelomic blood-fliiid. This pericardial
space, although apparently derived from the original coalom,
is not in communication with the other spaces and blood-
vessels derived from the coelom ; it never (or perhaps in a
very few instc u les) contains in the o.dult the MoUuscan blood
or h^molymph, and is always in free communication with
the exterior through the tubes called vphridia (renal
organs). The eu:art receives symmetrically on each side,
right and left, a dilated vessel bringing aerated blood from
the ctenidia. Tliese dilated- vessels are termed the auricUs
of the heart, whilst the median portion itself, at the point
where these vessels join it, is termed the ventricle of the
licart (C, 1'). The vessel passing foro and aft from the
ventricle gives off a few trunks which open into spaces
of the ccelom, the so-called lacunae ; these are excavated in
every direction between the viscera and the various bundles
of fibrous and muscular tissue, and may assume more or
less the character of tube-liko vessels witli definite walls.
Plight and left opening into the pericardial ccelom is a
coiled tube, the farther extremity of which ojiens to the
exterior by the side of the anus. Tlicse two tubes (C, it)
are the symmetrically disposed nephiudia (renal organs).
The coMADs (ovaries or spermaries) are placed in the
mid-dorsal region of the coelom (C, t), and have their own
apertures in the immcdiato ueighboiuhood of those of Uie
nephridia. The apertures arc paired right and left, and so
are the ducts into which they lead ; but at present wc have
no ground for determining whether the gonid itself was
primarily in JIoUu-scs a paired organ or a median organ,
nor have we any well-founded conception as to the nature
of the ducts when present, and their original relationship
i Mollusca ((
.\. or CTiiton ; /.(., flbroiM
■eat blood-vessel ; ,;./., later-
C. or I- .^snrella ; letter*
Fm. 2.— Ctenidia of
tissue ; a.h.v.t afferent blood-vessel ,
ally paii-ed lamellfe. B. Of Sei'ia , letters ti
as iii A. D. Of Nucula; d, p&sitiou of axis witli bloo-i-vosscis ; n, inner;
6 and c, outer row of l.ninellx'. E. Of P.i;udiua ; i, Intestine running ranillol
witli tlic axis of tlie cteniJiuni and ending in the anus o ; br, rows of clon^^ate
processes con-esjionding to tlm two series of iauiell.B of the upper liguies
to the gonads. The genital ducts of some organisms are
modified nephridia, but the nature of those of Mollusca,
of Arthropoda, of Echinoderma, of Nematoidea, and of
some Vertebrata lias yet to be elucidated.
The disposition of the nerve-centres is highly character-
istic. There are four long cords composed of both nerve-
fibres and nerve-cells which are disposed in pairs, two right
and left of the pedal area or foot, two more doi-sally and
tending to a deqier position than that occupied by the
pedal cords, so as to lie freely within the culomic space
unattached to the body-wall. These are respectively the
PED.u, NERVTs-conDs and the ^^scERAL nerve-cords. The
latter meet and join one another posteriorly. A right and
left (D, g-i), and a median abdominal tjj.nb) ganglion are
placed on these cords, and from them are given off the
osphradial nerves which have special ganglia (;/.olf). In the
region of the iirostomium the pedal nerve-cords are enlarged
behind the moutli, forming the pedal ganglia {ff./'e), and
are united by nerve-fibres to one another. From this spot
they are continued forward into the prostomium, where
they enlarge to form the right and left cerebral ganplia (f/.c),
which arc united to one another by nerve-fibres in front of
SCHE3IATIC mollusc]
MOLLUSCA
637
the mouth, just as the pedal ganglia are behind it. The
right and left pedal ganglia are joined by transverse cords
to the right and left visceral cords respectively, the point
of union being marked on either side by a swelling (g.jil)
known as the pleural ganglion. The visceral nerve-cord
can also be traced up on each side beyond the pleural
ganglion to the cerebral ganglion. Thus we have a
nearly complete double nerve-ring formed around the ceso-
phagiis by the two pairs of nerve-cords which are in this
region drawn, as it were, towards each other and away
from their lateral position both behind and before the
stomodzeal invagination. AVhilst the swollen parts of the
nerve-tracts are termed ganglia, the connecting cords
are conveniently distinguished either as conncdivis or as
commissures. Commissures connect two ganglia of the
same pair We have a cerebral commissure, a pedal com-
missure ard a visceral commissure. Connectives connect
ganglia of dissimilar pairs, and we speak accordingly of
the cerebro- pedal connective, the cerebro- pleural con-
nective, the pleuro-pedal connective, and the viscero-
pleural connective.
An ENTERIC NERVOUS SYSTEM forming a plexus on tne
walls of the alimentary canal exists, but does not exhibit
cords and ganglia visible to the naked eye except in the
large Dibranchiate Cephalopods
Our schematic Mollusc is prowded with certain osOAlfS
OF SPECIAL SENSE. Tactile organs occur on the head in the
form of short cephalic tentacles, (a). Deeply placed are
r cliorion : ot\ oral euil of the blastopore ; r, aiul end of the blastopoi ..
A. Fonuatinu of the Diblastula by the fni'ngiuation of larger cells iQto tlie
area of Bitialler cells (op'-ical section). B. View of the same siMjcimcn fioin
the surface of invagination ; the smaller cells are seen at the periphery ; by
Olvlsion they will inniliply and extend themselves over the four lai-ger cell!
ci.les with tl:
ond i;toino<l.'euiu, the oiiii
ofau eujbr>-o a little oldi
of the foot ; the extremity, or, coincides with thi
Jte extremity, r, with the anns. D. Optical section
tbau A. E. Surface view of the same euibrj-o.
a pair of closed vesicles containing each a calcareoiu con-"
cretion and acting as auditor)' organs ; these are known as
ocTocYsTs (D, y). They are situated behind the mouth
in the foremost portion of the foot. At the base of each
cephalic tentacle is a pigmented eye-spot — the cephalic
eye (D, ic). The ospHRADiUM (U), or peculiar patch of
olfactory epithelium at the base of the ctenidium, has
already been mentioned.
To the scheme thus exhibited of the possible organization
of the ancestral Mollusc we shall now add a sketch of
the mode in which this form of body and series of internal
organs are developed from the egg.
The cgg-ceU of MoUusca is either free from food material
—a simple protoplasmic corpuscle — or charged with food
material to a greater or less extent. Tlioss ciies which
appear to be most typical — that is to say, wliich adhere to a
A^
Fia. 4.— Development of tlie Pond-Snail, Limntevt stag nalis {attar Lankester,
15). r, Hirective coiTUscle; bl, blastopore; tv, eudoilenn or enteric cell
layer ; ec, ectodenn or dcric cell-layer ; r, veluin ; m, mouth ; /, foot ; t, ten-
tacles ; fp, pore in the foot (belonging to the pedal gland?) ; vi/, the uianllft-
flap or limbus palliaUs ; sh, the shell ; I, the snb-pallial si>ace, here destined
to become the lung. A. First four cells resulting from the cleavage of the
original egg-cell. B. Side view of the same. C. Diblastula stage (see Sg. 3X
showing tlie two cell-layera and the blastopore. D, E. F. Trochosphere
stage, D older than E or F. G. Three-quarter view of a Diblastula, to show
the orifice of invagination of the endodenrt or blastopore, bl. H, I. VelJger
stage later than D. (Compare fig. 70 and fig. 72*'*).
procedure which was probably common at one time to all
then existing MoUusca, and which has been departed from
A B ^...r:^:^ 0
Fio. 5.— Early stages of dinsion of the fertilized egR-cell in Xcssa wttcihau
(from ball.-ur. *fier Uubrctzky), A. The egg-cell has divdcd into two
spheres, of which the lower contains more food -material, whilst the upper I»
again incompletely divided into two smaller spheres. Resting ou the divIU-
ing upper sphere are the eight-shaped "directive corpusclis." better called
" pn*^eminal outcast cells or apoblasts," since they arc ttc result of a cell-
. division which arlects the egg-ccU before it is impregnsted. and arc mera
refuse, destined to disappear. B. One of the two smaller spheres is reunited
to the lai-gcr sphere. C. Tlie sinplo 'siuall sphere has divided into two, and
the reunited mass has divi<led into two, of which one is oblong and practi-
cally double, as in B, D. E-ich of the four seginent-cclla gives rise by divi-
sion to a small pellucid cell. E. The cap of small cells Ji as increased la
n'-niilier bv rrpeate<l fnnuation of i»ellucid cells in the name way. and hy
division of those Hi-st fonne-l. The cap wUl spread over and tnclose the four
negtutiit-ctilis, as in (ig. 3, A, R
only in later and special lines of descent — show approxi-
C38
MOLLUSCA
fscriEMATic Moiitrso:
mately the following history. By division of tne egg-cell
(fig. 3, A, B ; Cg. 4, A, B ; and fig. 5) a mulberry-ma.s3 of
embryonic-cc'Js i.^; formRf) (Morula), which dilates, forming
a one-cell-layered sac (Blastula). By invagination one
Fio. 0. — Developmcut of the Oyster, Ostrea edulla (modified from Horst, 16).
A- BlRstula Btage (onc-cell-laycreU sac), with comineiicins invasin.ition of
the wall of the sac at It, the blastopore. B. Optical section of a somewhat
later stage, in wliich a second invagination has commenced— namely, LiiaL
of the fihell-gland ofc; bt, blastopore ; en, invagiuated endodemi (wall of the
future arch-enteron) ; cc, ectoderm. C. Similar optical section at a little
later stage. The invagination connected with the blastopore is now more
contracted, d ; and c«Us, nw, forming the niesoblast fiom which the ccelom
ar'l muscular and skeieto-tropliic tissues develop, are separated. D. Similar
section of a later stage. The blastopore, W, has closed ; the anus will sub-
sequently perforate the coiTespoudin^ area. A new ajiertui-e, m, the mouth,
has eaten its way into the invaginated endodemial sac, and the cells pushed
in with it constitute the stomodEeum. The shell-gland, st, ia flattened out,
and a delicate shell, s, appears on its surface. The cili.ited velar ring is cut
in tho scc*>n, 83 shown by the two projecting cilia on the upper part of the
figure. Tlie embryo is now a Trochospliero. E. Surface view of an embryo
at a period almost Identical witli tliat of D. F. Later embryo seen as a
transpareut object, m, mouth ; ft, foot ; a, anus ; e, intestine ; st, stomach ;
tp, velar area of the prostomium. Tlie extent of the shell and commencing
npgrowtli of the mantle-skirt is Indicated by a line forming a curve from a
toF.
K.B.— In this development, as In that of Plsldium (llgs. 150, 151), no part of
the blastopore persists either as mouth or as anus, but the aperture closes, —
tlie pedicle of invagination, or narrow neck of the invaginated arch-entei-on.
becoming the intestine. The mouth and tli ' anus are formed as independent
In-pushings, the mouth with stoinodfeuin llrst, and tlie short anal proctodaium
touch later. This Interpretation of the appearances is contrary to that of
Horst (16), from whom our drawings of the oj-ster's development are taken.
The account given by the American naturalist Brooks (19) differs greatly as
to matter of uct from that of Horst and appcurs to bo erroneous in some
portion of this sphere becomes tucked into the other — as
in the .prej)aratiou of a woven night-cap for the head (fig.
6, B ; fig. 7, aJ. The orifice of invagination (blastopore)
narrows, and we now have a two-cell-layered sac,— the
Diblastula. The invaginated layer is the enteric cell-layer
or eiidodenn , the outer cell-layer is the deric cell-layer or
ectoderm. The cavity communicaling with the blastopore
and lined by the cndodcnn is the arch-enteron. The blas-
topore, together with the whole" embryo, now elongates.
,The blastoiiore then closes along the middle portion of its
extent, which corresponds Avith the later developed foot.
At the same time the stomodasuta or oral invagination
forms around the anterior remnant of the blastopore, and
the proctodaniin or anal invagination forms around the
posterior lemcaiit of the blastojjwe. There are, Loweveri
variations in regard to the relation of the blastopore to the
mouth and to the anus which are probably modifications of
the original process described above. AJi examination of
figs. 3, 4, 5, 6, 7, and of others illustrative of the embryo-
logy of particular forms which occur later in this article,
is now recommended to the reader. The explanation of
the figures has been made very f;ill so as to avoid the
Fro. 7.— Development of the River-Snail, Paludtna vivlpara (after Lankestevv
17). dc, directive corpuscle (outcast cell) ; Of, arch-enteron or cavity line t
by the enteric cell-layer or endoderm ; bl, blastopore ; vr, velum or circlet
of ciliated cells ; dv, velar area or cephalic dome : sm, site of the as yet ua-
formed mouth ; /, foot ; ■m/'s, rudiments of the skeleto-trophic tissues : pi,
the pedicle of iuvflglnatlnn, the futui-e rectum ; shgl, the primitive shell-sac
or shcU-gland ; m, mouth ; an, anus. A. Diblastula phase (optical section).
B. The Diblastula has become a Trochosphere by tlie development of the
ciliated ring vr (optical section). C. Side view of the Trochosphei-e with
commencing formation of the foot. I). Further odv.anced Trochosphere
(optical section). E. The Trochosphere passing to the Veliger stage, doi-sal
view showing the formation of the primitive shell-sac. F. Side view of the
same, showing foot, shell-sac (shijl), velum (w), mouth, and anus.
^ A*.B — In this development the blasto)ioi-e i» uot ciou„..U^t . il |>en.;sts as
the anus. The mouth and st/'inodfp-im form independently of the blastoporv.
necessity of special descriptions in the text. Internally, by
the nipping off of a pair of lateral outgrowths (forming
part of the indefinable "niesoblast") from the enteric cell-
layer the foundations of the ccelomic cavity are laid. In
some Ccelom.",*-i these outgrowths are hollow and of large
size. In JloUusca they ar^ nrt hollow and large, which is
probably the archaic condition, but they consist at first of
a few cells only, adhcmnt to one another ; these cells then
diverge, applying themselves to the body-wall and to tho
gut-wall so as to form the lining layer of tho calomic
cavity. Muscular ti.^auc develops from deep-lying cells, and
the rudiments of the paired nerve-tracts from thickenirjs
of the deric-cell layer or ectoderm.
The external form lueunwliile p-sscs through highly char-
acteristic changes, which are on the whole fairly constant
throughout the Mollusca. A circlet of cilia forhis when tha
embrjo is still ncarlj- bpUericaJ (fig. 4, F j Cg. 6, E ; Cg. 7-
(LASSKS Am) OBDESS.j
MOLLUSCA
639
^), in an equatorial position. As growth proceeds, one
hemisphere remains relatively small, the other elongates and
enlarges. Both mouth and anU4 are placed in the larger
area ; the smaller area is the prostomium simply ; the cili-
ated band is therefore in front of the mouth. The larval
form thus produced is kno^vn as the Trochosphere. It
exactly agrees with the larval form of many Chaetopod
worms and other Coelomata. Most remarkable is its
agreement ■with the adult form of the ^Yheel animalcules
or Rotifera, which retain the prse-oral ciliated band as their
chief organ of locomotion and prehension throughout Ufe.
So far the young Mollusc has not reached a definitely
Molluscan stage of development, being only in a condition
common to it and other Ccelomata. It now passes to the
veliger phase, a definitely Molluscan form, in which the
disproportion between the area in front of the ciliated
circlet and that behind it is very greatly increased, so
that the former is now simply an emarginated region of
the head fringed with cilia (fig. 8 ; fig. 6, F ; fig. 7, F ;
and fig. 60, A). It is termed the " velum," and is fre-
quently drawn out into lobes and processes. As in the
Botifera, it eerves the veliger larva as an organ of loco-
Vn, 8.— "^cMger** embryonic form of jro!V,;^c.i (from Gflgenbanr). r, relnm ;
-C viscera, dome witll dependent mantle-skirt ; p, foot : I, cephalic tentacles ;
ep, operculum. A. Earlier, and B, later, Veliger of a Gastropod. C. Veli-
ger o; a Pteropod showing lobo-Uke prorepses A the velum and the great
paired outgrowths of the foot.
motion. In a very few Molluscs, but notably in the Com-
mon Pond-Snail, the emarginated bilobed velum is re-
tained in full proportions in adult life (fig. 70), havin?
lost its marginal fringe of specially long cilia and iu
locomotor function. The body of the Veliger is char-
acterized by the development of the visceral hump on
one surface, and by that of the foot on the other. Gro\vth
is greater in the vertical dor.so-ventral axis than in the
longitudinal oro-anal axis ; consequently the foot is rela-
tively small and projects as a blunt process between mouth
and anus, which are not widely distant from one another,
whilst the antipedal area projects in the form of a great
hump or dome. In the centre of tliis antinedal area there
has appealed (often at a very early period) a gland-like
_,depre.ssion or follicle of the integument (fig. 6, C, si- ; fig. 7,
E, F, sV ; fig- 60, B ; fig. 68, s/is ; fig. 72***, ss). This is
the primitive shell-sac discovered by Lankester (18) in 1 871,
and shown by him to precede the development of the perma-
nent shell in a variety of Mol'uscan tyjies. Tho cavity of
this small sac becomes filled by a horny substance, and then
Itjvery usually disappears, whilst a deUcate shell, commenc-
ing from this spot as a centre, forms and spreads upon tl-c
surface of the vifceral dome.
The embryonic shell-sac or shell-gland represent: in a
transient form, in the individual development of most
MoUusca, that condition of the shell-forming area v/hich
we have sketched above in the schematic Mollusc. In
very few instances (in Chiton, and probably in Lintas), as
we shall see below, the -Jtmifnc shell-sac is retained and
erdarged as the permanent shell-forming area. It is su'>-
planted in other Molluscs by a secondary shell-forming
area, namely, that afforded by the free siu-face of the
visceral hump, the shell-forming activity of which extends
even to the surface of the depending mantle-skirt. Accord-'
ingly, in most MoUusca the primitive slM is represented
only by the homy plug of the primitive sheU-saC. The
permanent shell is a new formation on a new area, and*
should be distinguished as a secondary shell.
The ctenidia, it ^vill be observed, have not yet been
mentioned, and they are indeed the last of the charac-
teristic Molluscan organs to make their appearance. Their,
posi;ible relation to the prae-oral and post-oral ciliated bands!
of embryos similar to the Trochosphere will be discu.^sed'
in the final section of this article dealing with the Polyzoa
and Brachiopoda. The Veliger, as soon as its shell begins
to assiune definite shape, is no longer of a form common
to various classes of MoUusca, but acquires chaiactera
peculiar to its class. At this point, therefore, we shall
for the present leave it.
SrsTEiUTTC Review op the Classes and Okdees ok,
MOLLCSCA.
We are now in a position to pass systematically in
review the various groups of MoUusca, showing in what
way they conform to the organization of our schematic
MoUusc, and in what special ways they have modified or
even suppressed parts present in it, or phases in the repre-
sentative embryonic history which has just been sketched.
It ktU be found that the foot, the sheU, the mantle-skirt,
aad the ctenidia, undergo the most remarkable changes of
form and proportionate development in the various classes
— changes which are correlated with extreme changes and
elaboration in the respective fimctions of those parts.
Li"ision of the Phylum into tivo Branches. — The MoUusca
are sharply divided into two great Unes of de?"ent or
branches, according as the prostomial region is aifophied
on the one hand, or largely developed on the othei.
The probabilities are in favour of any ancestral form —
the hj-pothetical archi-Mollusc which connected the ixol-
lusca with their non-Molluscan forefathers — having pos-
sessed, as do all the more primitive forms of Coelomata, a
weU-marked jirostoinium, and consequently a head. The
one series of MoUusca descended from the primitive head-
bearing Molluscs have acquired an organization in which
the Molluscan characteristics have become modified in
definite relation to a sessile inactive life. As the most
prominent result of the adaptation to such sessile life they
exhibit an atrophy of the cephalic region. They form the
branch LipocEPHiU.A — the mussels, oysters, cockles, and
clams. The other sei'ies have retained an active, in many
cases a highly aggressive, mode of life ; they have, corre-
spondingly, not only retained a well-developed head, but
have developed a suecial aggressive organ in connexion
with the mouth, which, on account of its remarkable nature
and the pecuUarities of the details of its mechanism, serves
to indicate a very close generic connexion between fiU such
animals as possess it. This remarkable organ is the odon-
tophore, consisting of a lingual ribbon, rasp, or radula,
with its cushion and muscles. On account of the pos-
session of tills organ this great branch of the McUuscan
phylum may be best designated OLOSSOFHoaA. Any tena
640
MOLLUSCA
[classes and oedeks.
which merely points to the possession of a head is objec-
tionable, since this is common to them and the hypotheti-
cal archi-Mollusca fi'om wliich they descend. The term
Odontophora, wliich has been applied to them, is also un-
suitable, since the organ which characterizes them is not a
tooth, but a tongue.
1 \ " V
e J- »i;-j^ — 1_^ 'f /•
/
^0. 9 Odontophom of Glossophoroua MoUusca. k .* .
A. Diagram showing mouth, resophagus, and lingual apparatus of ftCnsfro-
pod in section, aa, upper lip ; al, lower lip ; h, calcarco-corneous jaw of
left side ; c, outer surface of the snout ; d, (esophaguG ; e, fold in the
vail of the ttsophagus behind the radular sac (a) ; /, anterior termina-
tion of the radnla and its bed, the point at which it weai-s away ; j,
liase of the radular sac or recess of the pharjTix : ft, cartilagmoua piece
developed in the floor of the pharynx beneath the radula, and serving
for the attachment of numerous muscles, and for the support of the
t&dula ; i, anterior muscles ; it, posterior muscles attached to the carti-
lage ; /, muscle acting as a retractor of the buccal mass ; to, muscle
attached to the lower lip ; n, posterior extremity of the radular sac ;
0, the bed of the nvdula or layer of cells by which its lower surface is
formed ; p, the horny radiUa or lingual i-ibbon ; q, opening of the radular
sac into the pharynx or buccal cavity ; r, cells at the extreme end of
tho inner surface of the radular sac which produce as a "cuticidar
> iwrru'.ion '■ liio rows of teeth of tho upper surface of tho rodula.
B. Badula or lingual ribbon of Pafudiaa vivipani, stripped from Ita bed,— a
homy, cutlcular product.
C. A single row of teeth fiom tho radula of Trochul civcrarlvs. lihlpldo-
glossate; formula. X.S.I.5.X.
D. Asinglo row of teeth from tho radula of TauUimafragUh. Ptenoglosaate ;
formula, x.O.x.
E. A Binglo row of teeth from tho raduhl of CMlim ciiiems. Tooelaborato
for formulation.
F. A single row of teeth fi-om tho radnla of Patella v:tlanla. Formula, S.l. 4.1.3.
O. A alr-slo row of teeth from Uio radula of Cui'riva hcli'ola. TaDnioglossato ;
fonnula, 3.1. s. „ . . ,
H. A single row of teeth finm tho radula of Nassa anmhin. Bacbiglossat^ :
formulii, l.I.l. Tho Cummon Whelk is similar to this.
Tho general stnictm-e of the odontopliore ( = too*b-
bearcr, in allusion to tho rasp-like ribbon) of tho plosso-
phorous MoUusca may bo conveniently described n-t once.
Essentially it is a tube-like outgrowth — tho radular sac (fig.
It, A, y, n)—\n tho median line of the ventral floor of tho
utomodicum, upon the inner siu-face of which is formed a
chitmous band (tho radula) beset with niiuuta teeth like a
rasp (/)). Anteriorly the ventral wall of the diverticulum
is converted into cartilage {h), to which protractor and re-
tractor muscles are attached (/-, t), so that by the action of
the former the cartilage, with the anterior end of the ribbon
resting firmly upon it, may be brought forwa;d into the
spaco between tho lips of the .oral aperture 'att, at), and
made to exert there a backward and forward rasping action
by the alternate contraction of retractor and protractor
mascles attached to the cartilage. But in many Glosso-
phora {e.g., the Whelk) the apparatus is complicated by the
fact that the diverticulum itself, with its contained radula,
rests but loosely on the cartilage, and has special muscles
attached to each end of it, arising from the body wall ;
these muscles pull tho whole diverticulum or radular sac
alternately backwards and forwards over the siu-face of the
cartilage. This action, which is quite distinct from tho
movement of the cartilage itself, may be witnessed in a
Whelk if the pharynx be opened whilst it is alive. It has
also been seen in living transparent Gastropods. The chi-
tinous ribbon is coutinuously growing forward from the
tube-like diverticulum as a finger-nail does on its bed, and
thus the wearing away of the part whicli rests on the car-
tilage and is brought into active ijse, is made up for by
the advance of the ribbon in the same way as the wearing
down of the finger-nail is counterbalanced by its own for-
ward growth. And, just as the new substance of the
finger-nail is formed in the concealed part, sunk posteriorly
below a fold of skin, and j-et is continually carried forward
with the forward movement of the bed on which it rests,
and which forms its undermost layers, so is the new sub-
stance of the radula formed in the compressed extremity
of the radular sac {n), and carried forward by the forward
movement of the bed (o) on which it rests, and by which
is formed its undermost layer. Tliis forward-moving bed
is not merel}' the ventral wall of the radidar diverticulum,
but includes also that portion of the floor of the oral cavity
to which the radula adheres (as far forward as the point /
in fig. 9, A). At the spot where the radula ceases, the for-
ward growth-movement of the floor also ceases, just as in
the case of the finger-nail the similar growth-movemeut
ceases at the line where the nail becomes free.
The radula or cuticular product of the slowly-moving
bed can be stripped off, and is then found to consist of a
ribbon-like area, upon which are set numerous tooth-like
processes of various form in transverse rovs, which follow
one another closely, and exactly resemble one another in the
form of their teeth (fig. 9, B). The tooth-like processes in a
single transver-'^o row are of very difl'erent shape and num-
ber in different members of the Glossophora, and it is pos-
sible to use a formula for their description. Thus, when
in each row there is a single median tooth with three teeth
on each side of it more or less closely resembUng one
another, as in fig. 9, G, we write the formula 3.1.3. When
there are additional lateral pieces of a different shape to
those immediately adjoining the central tooth, we indi-
cate them by tho figure 0, repeated to rejjresent their
number, thus 0000.1.1.1.0000 is tho formula for tho
lingual teeth of Chiton Stdleri. ■ A single median tooth,
an admedian scries, and a lateral series may be thus dis-
tinguished. In some Glossophora only median teeth are
present, or large median teeth with a single sm.dl ad-
median tooth on each side of it (fig. 9, H) ; these aro
termed Rachiglossa (formula, — .1. — or 1.1.1). 'In a large
number of Glossophora wo have three admedian on each
side and one median, no lateral jiieces (fig. 9, G) ; these
are termed Ttenioglossa (formula, 3. 1.3). Those with nume-
rous lateral pieces, four to six or more admedian pieces,
and a median piece or tooth (fig. 9, C) are termed Ehipi
doglossa (formula, x.6. 1.6.x, where x stands for an inde-
finite number of lateral pieces). Tho . Toxoglossa have
IBOFLEnBOUS aASTBOPODS.]
M 0 L L U S 0 A
641
1.0.1, the central tooth being absent and the lateral teeth
peculiarly long and connected with muscles. The term
Ptenoglossa (fig. 9, D) is applied to those Glossophora
in which the radula presents no median tooth, but an
indefinite and large number of admedian teeth, giving
the formula x.O.x. When the admedian teeth are inde-
finite (forty to fifty), and a median tooth is present, the
term Myriaglossa is applied (formula, x.l.x). It must be
understood that the pieces or teeth thus formulated may
themselves vary much in form, being either flat plates, or
denticulated, hooked, or spine-lilie bodies. We shall revert
to the terms thus explained in the eystematio descriotions
of the groups of Glossophora.
The muscular development in connexion with the whole
buccal mass, and with each part of the radular apparatus,
is exceedingly complicated, — as many as twenty distinct
muscles having been enumerated in connexion with this
organ. In addition to the radula, and correlated with its
development, we find almost universally present in the
Glossophora a pair of horny jaws (usually calcified) de-
veloped as cuticular productions upon the epidermis of the
lips (fig. 9, A, b). The radula and the shelly jaws of tlie
Glossophora enable their possessors not only to voraciously
attack vegetable food, but the radula is used in some in-
stances for boring the shells of other MoUusca, and the
jaws for crushing the shells of Crustacea, and for wound-
ing even Vertebrata.
'Pim.xni MOLLUSCA.
Branch k.— GLOSSOPHORA.
Cliaracters. — MoUusca with head-region more or less
prominently developed ; always provided with a peculiar
rasping-tongue — the odontophore — rising from the floor of
the buccal cavity.
The Glossophora comprise three classes, chiefly distin-
guished from one another by the modifications of the foot.
Class I.— OASTKOPODA.
Characters. — Gl&ssophora in which (with special excep-
tion of swimming forms) the foot is simple, median in
position, and flattened so as to form a broad sole-like sur-
face, by the contractions of which the animal crawls, often
divided into three successive regions — the pro-, meso^, and
meta-podinm — by lateral constrictions.
The Gastropoda exhibit two divergent lines of descent
hidicated by the term sub-class (see p. 649).
Sub-class 1.— GASTROPODA ISOPLEUKA.
Characters. — Gastropoda in which not only the head
and ioot but also the visceral dome with its contents and
the mantle retain the primitive bilaterai, symmetry of
the archi-Mollusc. The anus retains its position in the
median line at the posterior end of the body. The whole
visceral mass together with the foot is elongated, so that
the axis joining mouth and aniis is relatively long, whilst
the dorso-pedal axis at right angles to it is rhort. The
CTENIDIA, the NEPHRIDIA, GENITAL DUCTS, and CIECtTLA-
TORY ORGANS are paired and bilaterally symmetrical. The
pedal and visceral nerVe-cords are straight, parallel with
one another, and all extend the whole length of the body ;
the ganglionic enlargements are feebly or not at all deve-
loped. The Isopleura comprise three orders.
Order 1. — Polyplacophora (the Chitons).'
Characters. — Gastropoda Isopleura with a metameric re-
petition of the shell to the number of eight. The shells of
the primitive type are partially or wholly concealed in shell-
sacs comparable to the fsingle embryonic shell-sac of other
Mollusca. On the surface of the mantle-flap numerous
calcified spines and knobs are frequently developed. The
ctenidia are of the typical form, small in size and meta-
mencally repeated along the sides of the body to the
^'?;A°-~P"? ^f;!" of ^Chiton. A. Dorsal view of Chttm WosnessmkHi.
Midd., showing the eight sheUs. (After Middendorf.) B. View from tbi
pedal surface of u species of Chiton from the Indian Ocean » foot • o
mouth (at the other end of the foot is seen the anus raised on a papilla) • V
oral fringe ; 6r, the numerous ctenidia (branchial plumes) ; spreading beyond
these, and all round the animal, 13 the mantle-skirt (After Cuvier ) C Th»
same species of Chiton, with the shells removed and the dorsal litegtiuent
reflected. 0, buccal mass ; m, retractor muscles of the buccal mi^s • ov
ovary; od, oviduct; i, coils of intestines: ac. aorta; c", left auricle'- e!
ventricle, * ^
number of sixteen or more; an ospnradium or area of
" olfactory epithelium " (Spengel) is found at the base of
each ctenidium. The other organs are not subject to
metameric repetition. The odontophore is highly devel-
oped; the teeth of the lingual ribbon are varied in form,
several in each transverse row (fig. 9, E). Paired genital
ducts distinct from the paired nephridia are present.
The order Polyplacophora contains but one family, the
Chitonidx, with the genera: Chiton, Lin. (figs. 10, 15, &c.);
CryptochUon, Midd., 1847; and Cryptoplax ( = ChitonellusS'
Blainv., 1818. '
Order 2. — Keomenis.
Characters. — Gastropoda Isopleura devoid of a shell,
which is replaced by innumerable microscopic calcified
plates or spicules set in the dorsal epidermis ; mantle-flap
not lateral, but reduced to a small collar surrounding the
FlO. \\.—Nfmie:
Ventral view. C. Dorsal
men. a, anterior; 6, postei
foot is concealed.
B C
nata, Tullberg (after Tullbcrg).
' ■ D. Ventiaaviewofi
extremity; c, furrow, ia iTbicb the uanov
anus; ctenidia represented by a symmetrical group of bran-
chial filaments on either side of the anus; foot very nanow,
sunk in a groove; odontophore feebly developed, but the
radula many-toothed ; gonads placed in the pericardium
discharging by the nephridia ; no special generative ducts.
The order Neomeniae contains the two genera Keotnenia,
Tullberg (Solenopus, Sars) (fig. 11); and Pronennenia,
Hubrecht.
Order 3. — Chstoderma.
Characters. — Gastropoda Isopleura devoid of a shell,
which is replaced by numerous minute calcareous spines
Fio. li.—Chvtadcmr. nUidvXvm, Loren (after Graff). The cephalio enlarga-
ment is to the le't, the anal chamber (i-educed pallial chamber, containijig
the concealed pair of ctenidia) to the right.
standing up like hairs on the surface of the body ; body
XVL — 81
642
MOLLUSCA
[ISOPLEUKOUS GASTKOPODS.
much elongated so as to be vennifonn ; mantle-flap as in
NeomcnioQ ; ctenidia in the form of a pair of branchial
p'omcs, one on each side of the anus ; foot aborted, its
position being indicated by a longitudinal furrow ; odonto-
phoro greatly reduced, the radula only represented by a
single tooth ; gonads and nephridia as in Neomenia.
Tho ordei Chaetodenna contains the Bingle genus Chx-
toderma (fig. 12).
Farther remarks on the Isophurous Gastropods. — The
imion of the Chitons with the remarkable worm-like forms
Neomenia and Choetoderma was rendered necessary by
Hubrecht's discovery (25) in 1881 of a definitely consti-
tuted radula and odontophore in his new genus Proneo-
menia, founded on two specimens brought from the arctic
regions by tho Barents Dutch expedition.
By some writers — e.g., Keferstein — the Chitons have been
too intimately associated with the other Gastropoda, whilst,
on the other hand, Gegenbaur seems to have gone a great
deal loo far in separating them altogether from the other
lloUusca as a primary EUudivision of that phylum, inas-
much as they are inti-
mately bound to the
other Glossophora by
tho possession of a
thoroughly typical
and well - developed
odontophore. They
undoubtedly stand
.J nearer to tho archi-
MoUusca than any
other Glossophora in
having retained a com-
plete bilateral eym-
metry and the primi-
tive shell-sac, though
the metanaeric repe-
tition of this organ
and of the cteuidia is
a complication of, and
departure from, the
primitive character.
It is not improbable
that in the calcareous
spines and plates of
the dorsal integument
of Neomenia andChss-
toderma, which occur
Tiff. :3.-.>^Dl!iCT!mis nf th" allmmliry <anal of also on the part of
Isopleura (from Hubrecht). o, mouth ; a, tlig dorsum uncovered
anus ; d, alimt-ntary canal ; I, liver (digestive , in- r^i -i
gland). A. Neomenia and Proncomcnia. B. by shell in Lhlton, we
Chsttodcnna. c. Chiton. ^^^.q the retention of
a condition preceding the development of the solid Mol-
loscan shell, or a rever.sion to it. The minute calcareous
todies may have the same relation to a compact shell which
the shagreen denticles of the sharks have to a continuous
dermal bone.
The anatomy of tho Gastropoda Isopleura has been largely
elucidated within the past year by the researches of
Hubrecht and of Sedgwick, who have been the first to
apply the method of sections to the study of this group.
The leading points in tho modifications of mantle-flap,
foot, and ctenidia are set forth in the preceding summaries,
and in the accompanying references to the figures. \Vith
regard to other organs, we have to note the form of
tho alimentary canal (fig. 13), which is sim))!est in
Chaetoderma, symmetrically sacculated in Neomenia, and
wound upon itself, forming a few coils, in Chiton. The
latter has a compact liver with arborescent duct, which is
lepresented by the sacculi in Neomenia and by a single
caecum in Chstodenna. Salivary glands are present in
Chiton and in Proneomenia. The radula is highly devel-
oped in Chiton, and, though present in Proneomenia, has
not been described in Neomenia. A single tooth in Chs-
toderma appears to represent the radula in a reduced state.
The circulatory organs of Chiton alone are known with
any degree of detail (fig. 10, C). There is a median dorsal
blood-vessel — the aorta — which is enlarged to form a
ventricle in the posterior region of the body. On either
side the ventricle is connected to a weU-developed auricle,
which pours into it the aerated blood from the gills
(ctenidia). The extent to which vascular trunks are
developed has not been determined, but vessels to and
from the ctenidia, and in the mid-line 6i the foot, are
known. As in other MoUusca, the vessels do not extend
far, but lead into lacunce between the organs and tissues.
Dorsal and ventral vessels have been delected in Neomenia
and Chaetoderma, but no specialized heart.
Fia. H. — Diagrams of the excretory and reprodnctire organs of Isopleura (after
Hubrecht). 0, ovary ; P, pericardium ; K. nepliridium : u, external apcrturt
of nephritlium ; g. external aperture of the 5ri1it.1l duct of Chiton ; r, rectum;
CI, cloaca) or pallial chamber of Neomcniie and Cha:todenna ; Br. ctenidift
(branchial plujues). A. Cha:toderma. B^ Neomeoia. C. PToncomcnla. IX
Ihitoi
The heart of Chiton lies in a space which is to b«
regarded as a specialized part of tho coelom, and, as in
other Molluscs, is termed the pericardium. In front of
this space in Chiton lies the ovary (fig. 14, D). In the
other Isopleura the genital bodies (gonads) lie in the peri-
cardium, which has a longer form and extends dorsally
above the intestine. Opening into tlie pericardium equally
in all the Isoplcm-a (fig. 1 4) is a pair of bent tubes which
lead to the exterior. These are tho nephridia, which in
Chiton are essentially renal in function. Their disposition
has been determined by Sedgwick (26), who has shown that
each nephridium is much bent on itself, so that, as in the
ISbFLEDSOITS OASTSOPODa]
MOLLUSCA
643
Inephridia of Conchifera (organ of Bojanm), tne mtem&i
aperture lies near the external From the folded stem of
.the nephridium very numeroas secieting caeca are given o^
' — omitted in the dia-
gram (fig. 14, D), but
accurately drawn in
fig. 15. The sexes in
Chiton are distinct,
and the ovary or testis,
as the case may be,
though lying in and
filling a chamber of
the original ccelom,
does not discharge into
tine pericardium, but
has its own ducts,
■which pass to the ex-
terior just in front of
those of the nephridia
(fig. 14, D, g, and fig. ok
16). Li- this respect
Chiton is less primi-
tive than the other Iso-
pleuia, and even than
some other Gastropods
(the Zygobranehia),
'and some Conchifera
(Spondylus, (fee.), which
have no special genital
apertures, but make use
of the nephridia for
this DUTDOSe. InCTtton ^'m- is.— DissecUon of tha renal orgaM fneph-
J. * * . 1-1. ridia) of CAiton ncttZiii, after Haller Mroeiffn,
ducrepans, in which Zooi. /nsli/., Vlemii, 18S2X F, foot ; i, edge of
there are sixteen pairs S° ™"-'° "'°* removed ti the front pwt of
uuvAw (uo^tu.A.vvvu ^Mu«a i^Q gpecimen : ».o., cesophagus; o/, anoa; ffff,
of Ctenidia, the orifices genital dact: ^.external opening of the same;
^t 41..^ k-..^.:]:.^ «-« 'y- Btem of the nepbridimi^ leading to no, ita
of the nephndia are external apertnre ;«*, reflected portion of the
coincident with the six- oephridial stem ; nj, ene caeca of the nephh-
, . f . .J. dium, which are seen ramifying transrersely
teenth pair Ot Ctemdia, over the whole inner smi^oe of Uie pedal mos-
thoSe of the pnital 'ularmasa.
ducts with a point between the thirteenth and fourteenth
ctenidia.
In the Keomenisa and Chstoderma the nephridia are
'r^
short and wide (N in fig. 14, A,
B, C), and function as excretory
ducts for the genital products, the
gonads being lodged in the long
j>ericardium. Their separate or
united apertures open near the anus
into the small chamber formed by
the restriction of the mantle-skirt
to the immediate neighbourhood of
the anus
The nervous system of the Gas-
tropoda Isopleura is represented in
the diagram fig. 17. In all it is
important to observe that nerve-
ganglion cells are by no means
limited to special swellings — the
ganglia — but are abundant along
the -./hole course of the four great
longitudinal trunks. This is a pri-
mitive character comparable to that
fa. 16.— 6rar7 and oridncta presented by the nerve-cords of Ne-
l^f/i^.rSf'Sf^tS^^mertine worms, and of the Arthrol
and posterior snspensor of pod Peripatus. ffigher difTeren-
iB^'^Srt of'oTiduct); o, ti^tion in. other Mollusca leads to
"'^'*''''' predominance if not an exclusive
presence of nerve^/J&rej in the cords, and of nerve.^an^/it>n
cdh in the specialized ganglia. The numerous transverse
connexions of the pedsJ nerve-cords in Chiton and Neo-
menia (seen also in Fissurella (fig. 36) and some other
Gastropods) are comparable to the transverse connexions,
of the ventral nerve-
cords of Chaetopod
worms and Arthro-
pods. In the abund-
ance of the nervous
network connected
with it3 longitudinal
nerve-tracts, Chiton
appears to retain som3-
thmg of the early con-
dition of the Coelo-
mate nervous ^stem
when it had the form
of a sub-epidermic net-
work or nerve -tunic
(seen more clearly in
Planarians and some
Nemertines), and when
the concentration into
definitely compacted
cords had not set in.
Ganglia are, how-
ever, distinguishable
upon the nervous cords
of Chiton (fig. 18). The
cerebral ganglia are
not distingmshable as
«uch, but a pair of
buci^ ganglia (B in
fig. 18) are developed
on two connectives
which pass forward
from the cerebral re-
gion to the great mus-
cular mass of the
moutL These buccal
ganglia are special de^
velopments connected
with the special mus- ^£<,",;„ (^
CUlanty of the ups and hral ganglia ; s, anbllngnal ganglia ; «, pedal
odontophore, and are <eSS"f1i.'^S^'jL1Sffe'>£SS
found in all GloSSO- nerre-corda. A. Proneomeniau B. Neomenia.
1 I , . • . 1. C Chxtoderma. D. Chiton.
phora, but not m the
lipocephala. Such special ganglia related to special
organs (and not introduced in our schematic MoUusc, fig.
1) we find in connexion with
the siphons of the Lipoce-
phala, and in various posi-
tions upon the visceral nerve-
cords of other Mollusca, both
Glossophora and Lipocephala.
A pair of pedal ganglia but
little developed (p in fig. 18),
and a special group of sub-
lingual ganglia are present in
Chiton. On the whole, the
nervous system of the Iso-
pleura is exceedingly simple
and archaic, whilst it does not
well serve as a type with
_ which to compare that of
de- other Mollusca on account of'
tail(fro'mGegenhaur,£Z«nfn^o/Coii«9. ^. ,, ^ ^z ^ -.._
AiuLUmi^. B, bociai ganglia (con- the Small amount Of conceo-
""bii'^* ^'' °*°p°SdS'' '^' tration of its nerve-ganglion
glionand commcnceme'ntof pedal cells into ganglia, SUCh as WO'
??,7su°b2i^ ^3S'aSrn"°ift:find weU developed in other
♦"^i- forms.
The development of Neomenia and Chatoderma from
644
M O L L U B C ^i
[ANlSOPLEnBOUS CASTEOPODa
the egg is entirely nnknovm, that of Cliiton only par-
tially. Impregnation is effected when the eggs have been
discharged and are lying beneath the mantle-skirt. A
frochosphere larva i^J developed from the Diblastula of
Chiton (Loven).
The Chitons are found in the littoral zone in all parts of
the world, and are exclusively marine. Neomenia, Proneo-
menia, and Chictoderma have hitherto been dredged from
considerable depths (100 fathoms and upwards) in the
North Sea, Proneomenia also in the Mediterranean(Marion).
Sub-class 2.— GASTROPODA ANISOPLEURA.
Characters. — Gastropoda in which, whilst the head and
loot retain the bilateral sjinmetry of the archi-MoUusca,
the visceral dome, including the rnantle-flap dependent from
it, and the region on which are placed the ctenidia, anus,
generative and nephiidial apertures, have been .subjected
to a ROTATION tending to bring the anus from its posterior
median position, by a movement along the right side,
forwards to a position above the right side of the animal's
neck, or even to the middle line above the neck. This
toriion is connected mechanically with the excessive vertical
g-owth of the viscera! hump and the development upon
its sm'face of a heavy shell. The shell is not a plate en-
closed in a shell-sac, but the primitive shell-sac appears
and disappears in the course of embryonic development, and
a relatively large nautiloid shell (with rare exceptions)
develops over the whole surface of the visceral hump and
mantle-skirt. Whilst such a shell might retaiu its median
position in a swimming animal, it and the visceral hump
necessarily fall to one side in a creeping animal which
csjries them uppermost.
The .shell and visceral hump in the Anisopleura incline
Fio. 19. — Diagram to Ehow the effect of torgion 01 rotation of the visceral
hump In Gastropoda, when the visceral neire commissure passes above the
intestine ; A, unrotated ancestral condition ; T; quarter-rotation ; C, com-
plete Bemi-rotation (the limit) ; L, left, R, right side of the
normally to the right side of the animal. As mechanical
results, there arise a one-sided pressure and a one-sided
strain, together with a one-sided development of the
muscular masses which are related to the shell and foot.
I'.nth the TORSION THROUGH A .SEMICIRCLE of the base of the
visceral dome and the continued leiotropic sjiiral gro^lh
of the visceral dome itself, which is very usual in the
Anisopleura, appear to be traceable to these mechanical
conditions. Atrophy of the representatives on one side
of the body of paired organs is very usual. Those placed
inimitively on the left side of the rectum, which in virtue
(if the torsion becomes the right side, are the set which suffer
(see fig. 1 9). Some Anisopleura, al ter having thus acquired
a strongly-marked inequilateral character in regard to such
organs as the ctenidia, ncphridia, genital ducts, heart, and
fctum, appear by further change of conditions of growth to
have acquired a superficial bilateral symmetry, the second-
?.ry nature of which is rsreaicd by anatomical examination
(Opisthobranchia, Natantia).
In all groups of Anisopleura examples are numerous in
which the shell is greatly developed, forming a " house "
into v.'hich the. whole animal can be with-
drawn, the entrance being often closed
by a second shelly piece carried upon
the foot (the operculum). The power of
rapidly extending and of again contract-
J* ing large regions of the body to an
enormous degree b M ^
usual, as in the Li-
pocephalous Mol-
lusca. In spite of
the theories which
have been held on
this matter, it ap-
pears highly prob-
able that no fluid <
from without is in-
troduced into the
blood, nor is any ex-
l^eUed during these
changes of form.
A large mucous
gland with a med-
ian pore is usually ^
developed on the the streptoi
rebral ganglion ; Co^
pleural panghon . P, pe-
dal ganglion with otocj-st
attached ; y, pedal nerve;
A, abdom'inal ganglion
fit the extremity of the
twist€d visceral "loop" ;
sp, supra-intestinal v"
the foot, compar-
able to the simiilar
"of ApT^^tTal^TeTf gland and pore in
the long-looped Euthy- Lipoccphala, and in
neurousconditii.D. The / ti_
untwistedvisceraiioop some cases (e.^'.jPy-
IB lightly shaded, a, j-nla firr. 37, B) this ral ganglion on the course
cerebral ganglion ; pi, : """' "fa- "■'■"/ ""^ of the right visceral cord ;
pleural ganglion ; pe, liaS been mistaken s&,sub-intestinalganglion
pedal ganglion ; ah. sp, f ._ „ „.atpr nnrp °" "" '^""l' °^""' ij**
abdomin.al ganglion, ^""^ * ^^^'"P"'^^- visceral curd. (From Ge-
which represents also The leiotropic genbaur, after Jhcring.)
gangiicm"of '"sircpto- torsion of the vi.sceral dome has had
neuia and gives of! the igss deep -Seated efifect in one series of
nerve to the osphra- . . , , . , . j
dium (olfactory organ) Anisopleura than in another. Accord-
£rt"e?ed°°J'Sil:i°.g"e:ingly. ^s the loop formed by the two
nital" ganglion. Tlie VISCEKAL KEHVES (fig. 19) is Or is not
buccal nerves and can- i , •. • .r . • .
giin arc omitted. (Mter caught, as it Tvere, in the twist, we are
Spongei.) Q\y\Q to distinguish one branch or line of
descent with straight visceral nerves — the Ectthyneut-a
Fio. 22.— NrrT0U3 syetcm of tho Pond-Snail, Limnicus stagnalis, as a type of
tho alwrt-iooped Euthyneuroua condition. Tho sliort visceral "loop" with
(ts tliroo ganglia ts lightly-shaded. «, cerebral ganglion ; pt, pedal ganglion ;
p\, pleural ganglion ; ab, nbdominal ganglion ; sp, visceral panglion of the
left side; opposite to It is the visceral ganglion of tho riRht side, which
Rives off tho long ncr\e to the olfactory Raiiglion and o^pliradiom o. In
I'lanorbia and in Auricula (Pulnior\ata, alltna t*f LmmwHn) Uie olfactory oi^an
Is on tho Irfi sido and wcoives ita nerve from the Itjl visceral ganglioa
(After Spcngtd.)
(fig. 20) — from a second branch with the visceral nerves
rraoBRASCHiA.]
MOLLUSCA
645
twisted into a figure-of-eight — the SxREPTOlTEtrRA (fig. 21).
Probably the Euthyneura and the Streptoneura have de-
veloped independently from the ancestral bilaterally sym-
metrical Gastropods. The escape of the visceral nerve-loop
from the torsion depends on its having acquired a somewhat
deeper position and shorter extent, previously to the com-
mencement of the phenomenon of torsion, in the ancestors
of the Euthyneura than in those of the Streptoneura. The
junction of the two halves of the visceral loop in the
Euthyneura is below the anus, and the loop is therefore
not caught by the intestine. In the Streptoneura the
junction is (as in the Isopleura) above the anus.
Branch a— STREPTONEURA (Spengel, 1881).
Characters. — Gastropoda Anisopleura in which the
visceral "loop" (the conterminous visceral nerves) em-
braces the intestine and therefore shares in the torsion of
the visceral hump, the right cord crossing above the left
•o as to form a figure-of-eight (see fig. 19).
The Streptoneura comprise two orders — the Zygo-
branchia and the A^ygobranchia.
Order 1. — Zygobranchia.
Characters. — Streptoneura in which, whilst the visceral
torsion is very complete so as to bring the anus into the
middle line anteriorly or nearly so, the atrophy of the
primitively left-side organs is not carried out. The right
and left ctenidia, which have now become left and right
respectively, are of equal size, and are placed symmetrically
on either side of the neck in the pallial space. Related
to them is a simple pair of osphradial patches. Both right
and left nephridia are present, the actual right one being
much larger than the left. Two auricles may be present
right and left of a median ventricle (Haliotis), or only one
(Patella). The Zygobranchia are further very definitely
characterized by the archaic character of absence of special
genital ducts. The generative products escape by the
larger nephridium. The sexes are distinct, and there is
no copulatory or other accessory generative apparatus.
The teeth of the lingual ribbon are highly differentiated
(Rhipidoglossate). The visceral dome lies close upon the
oval sucker-like foot, and is coextensive with its prolongar
tion in the aboral direction.
' Tte Zygobranchia comprise three families, arranged in two sub-
orders.
Sub-order 1. Ctenidiohranehia.
Character, — Large Jjaired ctenidia acting as gills.
Family 1. — Baliolidw.
Genera : ffaliotis (Ear-Shell, Ormer in Guernsey) ; mostly tropical ;
Teinotis.
Family 2. — FisaurclUdic.
Genera : Fisstirclla {Key-hole Limpet) (figs. 24, 36), Emarginula.
ParmophoTUs (fig. 25) ; mostly tropical.
Sub-order 2. PhyUidiobranchia.
aractorj.— Ctenidia reduced to wart-like papillae ; special 8ub-
pallial lameUoe, similar to those of the Opisthobranch Plcuio.
phyllidia, perform the ftmction of gills.
Family Z.—Patcllida.
Genera: Patella (Limpet, figs. 26, &c.), A'oa/Za (BouLct-Liupet),
Lcttia.
Further RemarTcs onZygobrawhia. — The Common Limpet
is a specially interesting and abundant example of the
remarkable order Zygobranchia. A complete and accurate
account of its anatomy has yet to be written. Here we
have only space for a brief outline. The foot of the
Limpet is a nearly circular disc of musciJar tissue ; in
front, projecting from and
raised above it, are the head
and neck (figs. 26, 30). The
visceral hump forms a low
conical dome above the sub-
circular foot, and standing out
all round the base of this dome
so as to completely overlap the
head and foot, is the circular
mantle-skirt. The depth of
free mantle-skirt is greatest iu
front, where the head and neck
are covered in by it. Upon
the surface of the visceral
dome, and extendirig to the
edge of the free mantle-skirt,
is the conical shell. When „ „ „ ,
,,,,., /u i ***J- 24.— Dorsal aspect of a specimea
tne snell is taKen away (best of Fissoreiia a-om whicii the sheu
efifected by immersion in hot S"'JZ 'TT/'J'^m' V''°,'"l"'
>• nor area of the mantle-skirt has
water) the surface of the vis- been longitudinally sUt and its sides
..»w^1 A^ « ;., t^.l^A t.^ v« reflected, a, cephalic tentacle; ^,
ceral dome is fouud to be f„ot; j, lett (archaic right) giiit
covered by a black -coloured plume ; t, reflected mantlellap ; a
. , ,. "^ i_. 1 V the fissure or hole in the mantle-flap
epitnelium, wnicn may be re- traversed by the longitudinal Inci-
moved, enabUng the observer Ss-^ .^plrt\«7''5!'';in" • ^''Jea
to note tlie position of some (arclmic right) aperture of nephri-
organs lying below the trans- ^>^ ^ i-- »''°"'- (O'l^toai.)
parent integument (fig. 27). The muscular columns (c)
attaching the foot to the shell form a ring incomplete in
front, external to which is the free
mantle-skirt. The limits of the
large area formed by the flap over
the head and neck (ecr) can be traced,
_ and we note the anal papilla show-
ing through and opening on the right
shoulder, so to speak, of the animal
into the large anterior region of the
sub-pallial space. Close to this the
small renal organ (i, mediad) and the
larger renal organ [k, to the right
and posteriorly) are seen, also the
pericardium {l) and a coil of the in-
testine (ini) embedded in the com-
pact liver.
On putting away the anterior p^rt
of the mantle-skirt so as to expose
the sub-pallial chamber in the region
of the neck, we find the right and
left renal papillse (discovered by Lan-
'Som thfpS'iur'Sci.''"™ kester (27) in 1867) on either side
tede? ir.Ve'S'tte tw,; ^^^ ^""^ P^P'"* (^S" '^^\ ''"' °° ^^
symmetrical Eiiu placed on If a similar examination be made
tie neck. (ffriglnaL) ^f jj^g -^^^ ^^^^ FissureUa (fig.
24, d), we find right and left of the two renal apertures
a right and left gill-plume or ctenidium, which by their
presence here and in Haliotis furnish the distinctive char^
acter to which the name Zygobranchia refers. In Patellaj
no such plumes exist, but right and left of the neck are>
seen a pair of minute oblong yellow bodies (fig. 28, d)j
which were originally described by Lankester as orifices
possibly connected with the evacuation of the geneiativa
646
MOLLUSCA
FZYGOBRANCHIA.
prcStiols. On accoimi of their position they were termed
by him tiie "capito-psdal orifices," being placed near the
juncticn of head and foot. Spengel (24) has, however, in
a meat ingenious way shown that thsss bodies are the repre-
sentatives of the typical pair of ctenidia, here reduced to a
mere rudiment. Neiirtoeach rudimentary ctenidium Spengel
Fio. 26.— The Common Limpet iPalcltcL mlgata) In Ita ehell. seen from tie pedn!
Eorface. x, y, the median antero-ponterior axi3 ; a, cephalic tentacle ; b,
planUr snr£ice of the foot ; c, frc-e edge of the Shell ; d, the branchial effe-
rent vessel carryiDg aerated blood to the auricle, and here jntermpting the
circlet of gill lamellEE • e, margin of the mantlc-3l:irt ; f, gill lamella (noj
ctenidia, bnt special pallial growths, comparable to those of Pleurophyllidia);
ff, the branchial efferent vessel ; ft, factor of the branchial advelient vessel ;
i. Interspaces between the muscuiar bundles of the root of the foot causing
tie separate areae seen in fig. 27, c (OriginaL)
has discovered an olfactory patch or osphradium (consisting
of modified epithelium) and an olfactory nerve-ganglion
(fig. 32). It will be remembered that, according to
Spengel, the osphra-
dium of Mollusca is
definitely and inti-
mately related to the
gill - plume or cteni-
dium, being always
placed near the base
of that organ; further,
Spengel has shown
that the nerve-supply
of this olfactory organ
is always'derived from
the visceral loop. Ac-
cordingly, the nerve-
supply affords a means
of testing the conclu-
sion that we have in
Lankester's capito- f 'O- 27.— Dorsal surface of the Limpet
, 1 , , . . . ^ , . from its ehell and deprives! of ita b
pedal bodies the rudi-
mentary ctenidia. The
accompanying dia-
grams (figs. 34, 35) of
the nervous systems of
Patella and of Haliotis,
iTOd
deprived of ita black pig-
mented epithelium ; the internal organs are
seen through the transparent body-wall, c,
muscular bundles forming the root of the foot,
and adherent to the shoU ; c. free mantle-
ekirt ; cm, tcntaculiferous niarom of the same ;
i, smaller (left) nephridiuni; i, larger (right)
nephridium ; I, pericardium ; ix, librous septum,
behind the pericardium ; n, liver ; int, intes-
tine ; ccr, anterior ai-ca of the mantle-skirt over-
as determined by Spen- i^"=6i"s the head (cephaUo hood). (Onsinai.)
gel, show the identity in the origin of the nerves passing
from the visceral loop to Spengel's olfactory ganglion of
the Limpet, and that of the nerves which pass from the
visceral loop of Haliotis to tho olfactory patch or osphra^
dium, which lies in immediate relation on the right and
on the left side to the right and the left gill-plumes
(ctenidia) respectively. The same diagrams sawe to de-
Limpet, vlth
halic tentacle^ b,"fi:ot; c, muficular snbstanca
fLirmin^' the root of the foot ; d, the capito-peda]
organs of Lankejter (=mdimentary ctenidia); «^
mantle-skirt ; /, papilla of the larger nephridium ;
g, anus : ft, papilla of the smaller nephridinm ; U
smaller nephridiiun ; Jfc, larger nephridium ; Z, peri-
cardium ; m, cut edge of the mantle-skirt; is
liver ; p, snout. (OriginaL)
moastrate the Strsptoneurons Qondition of tie visceral loop
in Zy^obranchia.
Thus, tJien, we find that the Limpet possesses a sym-
metrically-disposed pair of ctenidia in a rudimentary con-
dition, and justifies
its position among
Zygobranchia. At
the same time it pos-
sesses a totally dis-
tinct series of func-
tional gills, which
are not derived from
the modification of
the typical MoUa*-
can ctenidium.
These gills ere in
the form of delicate Fio. 28.
lamelhB (fig. 26,/),
which form a series
extending oom-
pletely roimd the
inner face of the
depending mantle-
skirt. This circlet of gill-lameUs led Cuvier to class the
Limpets as Cyclobranchiata, and, by erroneous identifica-
,• tion of them with
, 9s. \ I /" ^^ series of meta-
t'\ \ \ [ / . merically repeated
d \ \s«9ifex\^ i^— ctenidia of Chiton,
to associate the
latter Mollusc
with tho former.
The gill -lamella)
of Patella are
processes of the
mantle compar-
able to the plitit-
like folds often
FiQ. 29. — The same specimen viewed from the left observed On the
fi^nt, so as to show the sub-anal tract (/)of the f ^e ii,^ V,-q-,
larger nephridium, by which it communicates with rOOI 01 lllO Dran-
tlie pericai-dimu. o, mouth; other letlei-a as in fig. 28. chial chamber in
Other Gastropoda (e.g., Buccinum and Haliotis). They are
termed pallial gills. The only other Molluscs in which
they are exactly represented
are the curious Opistho-
branchs Phyllidia and
Pleurophyllidia (fig. 57).
In ttese, as in Patella, the
typical ctenidiii are aborted,
and the branchial function
is assumed by close -set
lamelliform processes ar-
ranged in a series beneath
the mantle-skirt on either
side of the foot. In fig. 20,
d the large branchial vein of
Patella brir-ging blood from
fcia-/-
IS seen ; where it crosses
the series of lamellx there
is a short interval devoid
of lamella.
The heai-t in Patella con-
' ir^alorganA
relation to th«
rectum and to the pericardium. / p^
pilla of the larger nephridinm ; g, anal
papilla with reclmn leading from it; h,
papilla of the smaller nephridium, wMch
13 only represented by dotted outlines;
I, pericardium indicated by a dotted out-
lino,— St its right side are seen tho two
rcno-pei-icardial pon?3 ; JT. tie sub-anal
sistS of a single 8,Uriclo (not tract of the h-irgo nephridium given off
TT 1- i- J T7" near ita papilla and seen through tho
two as m Haliotis and flS- unshaded smaUer nephridium; Uo,ati.
sureUa) and a ventricle ; the Si,,'.;;?^ 7 i'°^i t ^L^t,"^
' . .Ilia phndium; A5.t, left lobe of aame; ftxft
former receives tue blOOa posteilor lobe of same; fo.i, inferior
from the branchial vein, the "ob-vtaMral lobe of same. (Original.)
latter distributes it through a large aorta which soon leads
into iiregulai' blood-lacmue.
f!aOBBASCBlAj\
MOLLUSCA
047
The ezistance of two renal organs in Patella, and their
relation to the pericardium (a portion of the ccelom), is
section : r, lingual sac (radular sac) ; rd, radula ;
salivary gland ; «, dnct of same ; v, buccal cavity ; . „
ftdvehcnt vessel (artery) ; br.v, branchial efferent vessel (vein) ; bv, blood-
vesj;! ; odm, muscles and cartibsc of the odoutophore ; cor, heart wlthiu tlie
pcricardiam. (Origiual.)
important. Each renal organ is a sac lined with glandular
epithelioiu (ciliated cells with concretions) communicating
Pio. 8!.— A. Section In a plane vertical to the snrtice of the neck of Patella
through a, the rudiiDCntary ctenidium (Lankeater's organX and &, the ol-
factory epitheiium (osphradiuni) ; c, the olfactory (osphradial) ganglion.
(After Spengel.) R Surface view of a radiiucntiry ctenidium of Patella,
excised and viewed as a transparent object. (OriginaL)
with the exterior by its papilla, and by a narrow passage
with the pericardium. The connesion with the pericar-
6
Fro. C3.— Vertical eectlon in a plr.nc mnning right and left throogh the
anterior part of the visceral huini\of Patella, to show the two renal or^ns
._ 1 .L.i. openings into the pericardium, a, Urge or external or right renal
and the;
process of the same running ^\ow the intestine and lead-
ing by k into the poricaiTlimn ; 6, small or median renal organ; r, peri-
cardium ; </, rectum ; t, liver ; /, man)Tl'G3 ; p. epithelium of the dorsal sur-
face : A, reuai epithelium lining the rensl sacs ; /, aperture connecting the
amal! sac wiUi tiie pericardium ; t, aperture connecting the largo s-ic with
thepericardium. (Ftcm ,-.„ f,rigiaal diauing by Ur J. T. CucniuAam, Fellow
of (Jr.i«rsity College, Oxford.)
dium of ths smaller of the two renal organs was demon-
stiated by Lanke-ste:- in 1867, at a time when the fact
that the renal organ of the JloUcsca, as » rtua, opens mic
the pericardium, and is therefore & tyjjical nephridium,
was not known. Subsequent investigations (37) carried on
under the direction of the same ,
naturalist have shown that tha
larger as well as the smaller renal
sac 13 in communication with the
pericardium. The walls of the
renal sacs are deeply plaited and
thrown into ridges. Below the
surface these v.-alls are excavated
with blood-vessels, so that the sac
is practically a series of blood-ves-
seb covered with renal epithelium, ,_
and forming a mesh-work within
a space communicating with the
exterior. The larger renal sac (re-
markably enough, that which is
aborted in other Anisopleura) ex-
tends between the Kver and the
integument of the visceral dome no. st-Xervous system of ft-
very widely. It also bends round Jf'J?.,' ^t /"i^^l ''?'' '^
.1 •^v •' , • /! o/s , lightly shaded: the boccsl
tne liver as shown in ng. oO, and ganglia ara omitted. «, cero-
forms a la^ge sac on half of the mTige°f^,'p'icSS^6S;
upper surface of the muscular mass f- 1*^' eaugiion ; pe, pedal
of the foot. -Here it lies close feft) to'tb'e SSit^f o^o^
upon the genital body (ovary or ^Se^o^^iTsJ^Xn'^*^
testLs), and in such intimate rela- visceral loop. (After spengei.)
tionship with it that, when ripe, the gonad bursts into the
r«nal sac, and its products are carried to the exterior by
th^ papUla on the right side of the anus (Sobin, Dall).
This fact led Cuvier erroneously to the belief that a duct
existed leading from the jronad to this papilla. The
position of the gonad, best seen in the diacTammatic
Fio. 35.— Ncrrons system of Haliotis; the rlsccral loop li lightly shaded:
the buccal gauglia arc omitteil. cc, cc-^bial ganglion : pf.pf, the fused pletuaj
and pedal ganglia ; /w, the rigiit petlal nerve ; ce.pf, the cerebro-pleural
' "^ erebro-pedal cooueotive; », s",
; ah. abdomiual ganglie
I left
te of same ; o. o. right and left olfactoly
from visceral loop. (Ailer Spengel.)
u-.-i ,v3 , uv. aiiuuiiuuai gs.igiiun
pmglia and osphiadia receiving
section (fig. 31), is, as in other Zygobranchia, devoid of
a special duct communicating ■with the exterior. This
condition, probably an archaic one, distinguishes the Zyg»
brancliia among all Glossophorous iloUusca.
The digestive tract of Patelia offers some interesting
features. The odontophore is powerfully developed-j the
radular sac is extraordinarily long, lying (wiled in a eoei^
648
MOLLUSGA
[azvcobbahchii,
between the mass of the liver and the muscular foot. The
radula has 160 rows of teeth -svith twelve teeth in each tow.
Two pairs of salivary ducts, each leading from a salivary
gland, open into the buccal chamber. The cesophagxis leads
into a remarkable stomach, plaited like the manj^pUes of a
sheep, and after this the intestine takes a very large num-
ber of turns embedded in the yellow liver, until at last it
passes between the two renal sacs to the anal papilla. A
curious ridge (spiral t valve) which secretes a sUmy cord is
found upon the inner wall of the intestine. The general
structure of the JloUuscan intestine has not been suffi-
ciently investigated to render any comparison of this struc-
ture of Patella with that of other MoUusca possible. The
eyes of the Limpet (28) dessrve mention as examples of
the most primitive kind of eye in the MoUuscan series.
They are found one on each cephalic tentacle, and are
simply minute open pits
or depressions of the
epidermis, the epidermic
cells lining them being
pigmented and connected
with nerves (compare fig.
118).
The Limpet breeds
upon the soutliem Eng-
lish coast in the early
part of April, but its de-
velopment has not been
followed. It has simply
been traced as far as the
formation of a Diblastula
which acquires a ciliated
band, and becomes a
nearly spherical Trocho-
Bphere. It is probable
that the Limpet takes
several years to attain
full growth, and during
that period it frequents
the same spot, which
becomes gradually sunk
below the surrounding j.^^ so.-Semw system of Fissraella. j,!,
e ; p, pedal i
A; abdomi
lia in the Streptonenrous visceral
with supra- and Gub- intestine
__, ., jtocysts attached to the cerebro-
edal connectives. (Prom Gegenbaur, after
tering.)
surface, especially if the paiiiai
rock be carbonate of lime. ""_'"
At low tide the Limpet r.^ii°i.°S;,^°!;,?L*° lA,*.°S?;l i^^'^
(bemg a strictly inter-
tidal organism) is ex-
posed to the ail', and is
to be found upon its spot of fixation ; but when the water
again covers it, it (according to trustworthy observers)
quits its attachment and walks away in search of food
(minute encrusting algaa), and then once more as the tide
falls returns to the identical spot, not an inch in diameter,
which belongs, as it were, to it. Several million Limpets
— twelve million in Berwickshire alone — are annually used
on the east coast of Britain as bait.
Order 2. — Azygobranchia.
Charaaers. — Streptoneura which, as a sequel to the
torsion of the visceral hump, have lost by atrophy the
originally left ctenidium and the originally left nephriJium,
retaining the right ctenidium as a comb-like gill-plmno to
the actual left of the rectum, and the right ncphridiiun
(that which is the smaller in the Zygobranchia) also to the
actual left of the rectum, between it and the gill-plume.
The right olfactory organ only is retained, and may assume
the form of a comb-like ridge to the actual left of the
ctenidium or branchial plume. It has been erroneously
described as the second gill, and is known as the para-
branchia. The rectum itself lies on the animal's right
shodder. The prcaonce of {jianJiJar plication of the siufaca
of ihe m?.n'.\'>Z%i> (fig. 46, x) and an adrectal gland (purple-
gland, fig. 47, yji) are frequently observed. The sexes are
always distinct; a special gemtal duct (oviduct or sperm
duct) unpaired is present, opening cither by the side of the
anus or, in the males, on the right side of the neck in con-
nexion with a large peois. The shell is xisually large and
spiral; often an operculum is developed on the upper sur-
face of the hinder part of the foot. The dentition of the
lingual ribbon is very varied. In most cases the visceral
hump .and the foot increase along a:ses at right angles to
one another, so that the foot is extended far behind the
visceral hump in the ab-oral direction, whilst the visceral
hump is lofty and spirally t'^visted.
This is a very large group, and is conveniently divided
into two sections, the Reptantia and the Natantia. The
former, containing the immense majority of the group,
breaks up into three sub-orders, the Holochlamyda, Pneu-
monochlamyda, and Siphonochlamyda, characterized by the
presence or absence of a trough-like prolongation of the
margin of the mantle-flap, which conducts water to the
respiratory chamber (sub-pallial space where the gill, anus,
itc, are placed), and notches the mouth of the shell by
its presence, or again by adaptation to aerial respira-
tion. The sub-orders are divided into groups according to
the characters of the lingual dentition. In some Azygo-
branchia the mouth is placed at the end of a more or less
elongated .snout or rostrum which is not capable of intro-
version (Rostrifera) ; in the others (Proboscidifera) the
rostrum is partly invaginated and is often of great length.
It is only everted when the animal is feeding, and is with-
drawn (introverted) by the action of special muscles ; the
over-worked term " proboscis " is applied to the retractile
form of snout. The term " introversible snout," or simply
"introvert," would be preferable. The presence or absence
of this arrangement does not seem to furnish so natural a
division of the Reptant Azygobranchia as that afforded by
the characters of the mantle-skirt.
Section a.— REPTANTIA.
Characters. — Azygobranchia adtipted to a creeping life ; foot either
wholly or only the mesopodium in the form of a creeping disc
Sub-order 1. — Hotochlainyda.
Characters. — Reptant Azygobranchia with a simple marg^ to the
mantle-skirt, and, accordingly, the lip of the shell unnotched;
mostly Rosti'ifera (t.c, with a non-introversible snout), and vege-
tarian ; marine, bmckish, fresh-water, teiTestriaL
o. JViipidoglossa (x.4 to 7.1.4 to 7.x).
Family 1. — Trochidse.
Genera : TiirbOy Lin. ; Phasianclla, Lam. ; Tmperatorf MoDtf. j
Trochus, Lin. ; HotcUa, Lam. ; EuovijihahtSj Low.
Family 2. — Nfritidsj.
Genera : Ncrita, L. ; Ncrititxa, Lam, ; FiUolm, Low ; Navkclla,
Lam.
Family 3. — Plcurotomarida.
Genera: Plcurotomaria, Defr. ; Anatomus, Montf. ; Stomalia,
Helbmg.
/3. Ptenoglossa {,x.0.x).
Family i. — Scalaridee.
Genus : Scalaria, Lam.
Family 5. — Janthinidx.
Genera : JaiU/iina, Lam. (fig. ii) ; }!ecluzia. Petit
7. Teenioglossa (3.1.3).
Family 6.—Cer!lhidis.
Genera: Ccrilhinm, Brug.; Potamidcs, Brong.; Kerinaea, Defr.
Family 7. — Mctanidw.
Genera: Mdania, Lam.; Mclanopsia, Fir.; Ana/lotus, Lay.
Family 8. — PyramidclUdiu.
Genera: Pyramiddla, Lam.; Stylina, Flem.; Aclis, Loven.
Family 9. — furrilcUid«.
Genera: Turrilclla, Lam.; Ceectim, Flem.; Vemutus. Adans.;
Siliquaria, Brug.
Family 10. — Xcnophoridtv.
Genus : Phorus, Montf. (fig. 39).
(AZyGOBR ANCHIA. j
MOLLUSC A
T.1^ Tn^W 0, TEK Sm«)m3I0KS 0. TH. CLASS «-^^OPODA, AB^^o.::. so ^ «, aHOW THm «;i^S^ (toETX
Class. —GASTROPODA.
[Arch-isophurum. )
i L
64»
SulMjaSS 1. — ISOPIETBA.
Snb-cUs9 2. — AkisopIiEwea.
(ArchicuOiyneurum. )
Branch a. — SiEEPT0Ni;ur>4
(Archwygobrancldum. )
Branch i.— EuTHTNEiriLi.
(Arckiopisthobranchiwni. )
9 9 Q Order 1.— Sygobranchia.
Order 2. — ^AzraoBEANCHiA.
(Archilwlochlamydum. )
Sect. a.
SeptarUia,
Order 1.— Opisthobeascbia.
lArchipalliatum.}
2.— PULJ
Order 2.— Pulmonata.
Sect. a.
Palliaia,
Sect >.
NonrPalliata.
I i r
Family 11. — Naiicida.
Genera: If lUica, lam.-, Sitjarttus, tam.; Neritopsia, Gratel.
Family 12. — EntoconchicUe.
The single genus and s{)ecies Entoamcha mirdtnlis, discovered by
Joh. Miillcr in 18S1, parasitic in Synapta digiltUa. The adult
form is not known.
I'\imily 13. — Marscnidse.
Genera : Marscnia, Leach ; Ondiidiopsis, Beck.
Family 14. — Acmwidse.
Genera : Acnusa, Esclisch. ; Loltia, Gr. ; (probably these will be
found to belong to the Zygobranchia).
Tataily 15. — CopvAidse.
Genera : Capulus, Jilontf. ; Calyptrm,, Lam. (fig. 40) ; TrochUa,
Schum.
Family 16. — LiUorinidiv.
Genera : Littorina (the PeriwinWcs, fig. 46) ; Modulus, Gray ;
Lacvna, Turt. ; Missoa, Frem. ; Eydrobia, Hartm, ; Assiminia,
Leach.
Family 17. — Paludinidic.
Genera : Palv.dina (RiTer-SnaU) (figs, 7, 21) ; JBUhynia, Gray ;
Taialia, Gray.
Family 18. — Valmtidie.
Genus : Valmta (fij. 45), fresh-water.
Family 19. — AmpuUarUlss.
Genus : AmpuUaria (can breathe air by means of the ■walls of
the pallial chamber as well as water by the gill ; fresh-waters
of tropical .\merica, Africa, and East Indies).
Subrordcr 2. — PncumoiwcMamyda.
C/icrocJcrs. —Paffial chamber a lung-sac; no gill; mouth on a
rostrum, not a retractile proboscis; terrestrial habit
Famil? 20. — Cyclostomida.
Genera: Cydosloma, Lam.; CyclopJuirus, Montf.; FerusnTm,
GrateL ; ftgjina, Vjgnard.
Family 21. — Eelicinidx (radula ihipidoglossate rather than ttenio-
glossate). . TT 7. •
Genera : Stoastoma, Adams ; Trochatella, Swains. ; Heltana,
Lam.; Proserpina, Guild.
Family 22. — Aciailidm.
Genera : Adcula, Hartm. ; Oeomelania, Pfr.
Sub-order 3. — Siptionochlamyda.
Characters, — Eeptant Azygobranchia with the margin of the
mantle drawn out to form a tiough-liko sichon which notches the
lip of the shell ; shell always epix'al ; usually an operculum, homy
or lamelliform ; either a rostrum or a retractile proboscis ; exclusively
marine ; mostly carnivorous.
* Tanioglossa, (3.1.3).
Family 1. — Stromiidec.
Genera : Stromhus, L. ; Pkreceras, Lam. ; Bostellariai Lam.
(fig. 43).
Family 2. — Aporrhaidas.
Genus : Aporrhais, Da Costa.
Family 3. — Pedicularidw.
Genus : Pedicularia, Swains.
Family 4. — Dolidee.
Genera : Cassis, Lam.; Cassidaria, Lam.: Dolium, Lam.; Fiaita,
Swains.
Family 6. — Tritonids.
Genera : Tritonium, Cuv. (fig. 42) ; Eanclla, Lam.
Family 6. — Cyprmidae (the Cowries).
Genera : Cypresa, L. ; Owilum, Brag. (fig. 41) ; Erato, Eisso.
"Toxiglossa (1.0.1).
Family 7. — Conidm.
Genus : Conies, L.
Family 8. — Tercbrideg.
Genus : Tcrebra, Adans.
Family 9. — Plcuroiomidm.
Genus : Pleurotoma, Lam.
Family 10. — Cancellaridm.
Genus : CaTiceUaria, Lam.
* Sttchiglossa (1.1.1 or .1.).
Family 11. — Murtcidss.
Genera : Murcx, L. ; Trophon, Montf ; Pusus, Bmg. ; Pyrula,
Lam. (fig. 38); Turbinella, Lam.
Family 12. — Buccinids.
Genera: Buccinum, L.; Nassa, Lam. (fig. B); Purpura, Brag,
(fig. 47); ConchoUpas, Lam.; ilagilus, Montf.
I Family 13.— itUrida.
I Genua : Milra, Lam.
XVL — 83
650.
MOLLUSCA
y^:- o7!E AircmC*
Family ii.—Olivide.
Genera : Oliva, Brag. ; Andlla, Lam. ; Sarpa, Lam.
Family 15. — VolrUidw.
Genera : Valuta, L. ; Oymbivm, Montf. ; Margi'iiaHa, Lam. ;
Volvarui Lam.
Further Jtetnarh on the Reptant Azygo'.ra.nchia. — The
very large assemblage of foi-ms coming iijider this order
comprise the most highly developed predaoeous searsnails,
numerous vegetaiian species, a considerable number of
^W:!^-r^i-v7r--. ;
retractor muscle of t,ho foot, ■whioh cliugs t~ tbr; spiral
column or co'ujn:iUa of the shell (see Eg. 42). This col-
umella muscle is the sar:ie thing as the muscular Burfacs
marked c in the figures of Patella, marked h in fig. 91 of
Nautilus, and the posterior adductor of Lamellibranohs
(fig. 131).
The surface of the neck is covered by integument forming
the floor of the branchial cavity. It has not been cut inta'
<
Pio. 87. — A- TrUon varicgatum, to show tho proboscis
In a state of '
fold of the mantle-skirt . .
Ing on the ehell ; c, cephalic eye ; d, cephalic tcntacla
introvert (proboscis) ; / foot ; g, operculum
icgatum, to show tho proboscis or bnccai mtrovrjrt ^
a, siphonal notch of the shell occupied by the siphonai
rt (Si phono chlamyda) ; h, edge of the mantle-skirt rest-
' " ' . -■- -.--^--■.- - [^ everted buccal
wider snrfece of
tle'-skirt forming the roof of'the sub-pallial chamber. D. Sole of the
foot of Pyrula tu&a, to show a, the pore uaoally said to be "aqniferoua"
but probably the orifice of a gland ; b, median line of foot
fresh-water, and some terrestrial fcrms. The partial dis-
section of a malo specimen of the Coaunon Periwinkle,
Littorina liUoraliSy drawn in fig. 46, will serve to exljibit
the disposition of viscera which prevails in tho group.
<'^
5 (T, (t-.'jitl <not Introvereible); 1
ud laeao-podium,— to the right <
;ulptuiwi opsrcolmn.
Pio. St).— Animal mi shf 11 of Monu r-u.'i
cephalic tentacles ; c, Tight eye ; d, pro- !
thie is seen the metapoiiium bearing Lho e
Of the organs Ijing on the reflected mantle-skirt, that which
in the natural state lay nearest to the vas deferens on the
right side of the median line of
the roof of the branchial r hambar
is the rectum i\ ending in tho
anus a. It can be traced back to
the intestine t near the surface of
the visceral hump, and it is found
that the apex of the coil formed
by the hump is occupied by the
liver h and the stomach v. Phar
rynx and cjsophagus are con-
cealed in the hea/J. The enlarged
glandular structure of the walla
of the rectum is frequent in the
Azygobranchia, as is also though
not universally the gland marked
y, next to the rectum. It is the
adrectai gland, and in the genera
Hares and Purpura secretes a
colourless liquid which turns
Vm. 88.-AnlmaI and thel! of Fyrvla lanigala. a, siphon ; h, head-tentacles ; C, head, tho letter placed near the right PU^p's "^pon exposure to the at-
eye; ff, the foot, expanded as in crawling ;», the nmntle-skirtreaeoted over the sides of the shea (From Owen, mosphcrs, and waS USOd by tuO
he bi-duchial chamber formed by tho mantle-skirt over- ancients as a dye.
Near thi-j, and less
advanced into the
branchial chamber,
is the single renal
organ or nepbri
dium r with '
openinf; to tho i
terior »■'. Internally
this glandular sa ;
presents a second
slit or aperture
which leads into the
per;c-j-dium (oa is
n^ n found to be
the case in all Mol- to aii'
lusca). This heart '"'"
e lying in the pericardium is seen in close proximity tgj
hanging the head has been exposed by cutting along a line
extending backward from the letters vd to tho base of the
columella muscle mc, and the whole roof of the chamber
thus detached from the right side of the animal's neck has
been thrown over to the left, showing tho organs which lie
tipon the roof. No opening into the body-cavity has been
made; the organs which lio in the coiled visceral hump
show through its transparent walls. The head is seen in
front resting on the foot and carrying a median non-retractile
finout or rostrum, and a pair of cephalic tsntacltj at the
base of each of which is an eye. In many Gastropoda the
jyea are not thus sessile but raised upon special eye-tentacles
(figs. 43, 69). To the right of the head is seen the muscular
penis p close to the termination of the vas deferens (sper-
matic duct) vd. The testis I occupies a median position in
the coiled visceral mass. Behind the penis on the same
ude is tho hookliko columella muscle, a development of the
Shell of CalyptTffa, Fcen from below 60 a^
r tlic inner whcrl &, concealed by the cap*
IZTOOBRAKCHUll
MOLLUSC A
651
the renal organ, and consists of a single anricle receiving
blood from the gill, and of a single ventricle which pumps
it through the body by an anterior and posterior aorta
(see fig. 105). The
surface x of the
mantle between the
rectum and the gill-
plume is thrown
into folds which
in many sea-snails
(Whelks, &c.) are
very stronely deve-
\^J^A tS^ _v 1 Fro. 4J.— Ani'mal and slicU of Ovnloo. t, cepbaKo
lopea. ine Wnole Uutacles; d, foot; *, mantle-skirt. wWch is natu-
of this surface au- «Uy carried in e reflected conditioa so as to
. ^ cover in the sides of the EnelL
pears to be active
in the secretion of a mucous-like substance. The single
gill-plume br lies to the left of the median line in natural
position. It corresponds to the
right of the two primitive cten-
idia in the untwisted archaic
condition of the Molluscan body,
and does not project freely into
the branchial cavity, but its
asds is attached (by concres-
cence) to the mantle-skirt (roof
of the branchial chamber). It
is rare for the gill-plume of an
Anisopleurous Gastropod to
etand out freely as a plume,
but occasionally this more ar-
chaic condition is exhibited, as
in Valvata (fig. 45). Next be-
yond (to the left of) the gill-
plume we find the so-called para-
branchia, which is here simple,
but sometimes lamellated as in
Purpura ("-g. 47). This organ
has, without reason, been sup-
posed to repre3ent the second p,„ 42.-s!Jtion of th, d.eii' of
Ctemoiumot the typical Mollusc, Tritonium, Cut. o, apei ; oc, si-
which it cannot do on account L^uto" to^?L?n" hTttle'S-
of its position. It should be ". ". "horU of the shell ; s, s, sn-
^4.1 ■„!.* e i.1. turea. Occupying the axis, and
tne ngnt or tne anus were exposed by the section, is seen the
this the case. Recently Spengel r"'™'t,'^T"''7ff^k''n'^- '"'^
fc , . ^ t npper whorla of the shell are Been
nas shown that the parabran- to be divided into eeparate Cham-
;cWa of Gastropods is the typical STv^iy^o'JSed^se^S."' ff^S
olfactory organ or osphradium Owen.)
|in a highly-developed condition The minute structure
'of the epithelium which clothes it, aa well as the origin of
^a 48.— Animal and shell of Bost^Iarta rtetinstrU. a, snont or mstrum ;
t b, cephalic tent&cle ; c, eye ; d,^ropodinm and mesopodiom ; e, metapodinm ;
/, opercnlnm ; h', prolonged siphonal notch of the sheU occopied by the
i siphon, or trongh-ljice process of the nujitle-skirt. (From Owen-)
tie nerve which is distributed to the parabranchia, proves
jit to be the same organ which is found universally in Mol-
luscs at the base of each gill-plume, and te°ts the indrawn
current of water by the sense of smell. The nerve to thi»
organ is given off from the superior (original right, sea
fig. 1 9) visceral ganglion.
The figures which are here given of various Azygo-
branchia are in most cases suffi-
ciently explained by the refer-
ences attached to them. As an
excellent general type of the
nervous system, attention may
be directed to that of Paludina i
drawn in fig. 21. On the whole,
the ganglia, are strongly indivi-
dualized in the Azygobranchia,
nerve-cell tissue being concen-
trated in the ganglia and absent f,o. 45.— rajtmii mstaia, moil
from the cords (contrast with Zy- •>• "'.°9"' -yp- opercuinm ; br,
, ,. J T 1 \ *i ctcmdiom (branchial plume) ; *i
gobranctua and Isopleura). At SUform appendage (? rudiment-
the same time, the junction of jXTcSL!l"?,?fSrf?S
the visceral loop above the in- not having its axis fused to ti»
A. *;..„ „„.»„-, ;« „n c*. d. roof of the branchial chamber is
testine prevents m all StreptO- the notable character of thi»
neura the shortening of the vis- b"""-
cral loop, and it is rare to find a fusion of the visceral
ganglia with either pleural, pedal, or cerebral — a fusion
which cau and does
take place where the
visceral loop is not
above but below the
intestine, e.g., in the
Euthyneura (fig. 67),
Cephalopoda(fig.ll2),
and LameUibranchia
(fig. 144). As con- i
trasted with the Zygo-
branchia and the Iso-
pleura, we find that in
the A^gobranchia the
pedal nerves are dis-
tinctly nerves given off
from the pedal ganglia,
rather than cord-Uke
nerve -tracts contain-
ing both nerve -cells
or ganglionic elements
and nerve-fibres. Yet
in some Azygobran-
chia fPaludina) a lad- F">- 46.— Mala of Littorinn ttUmilis, Lin., n^
J ,:, ' moved from its shell; the mantle-skirt cut along
aer-llke arrangement its right Une of attachment and thrown over
nf tliB twn npdal to the left side of the aninml so as l« expose tha
01 tne two peaai organs on its inner face. a,anus ; (, intesUno;
nerves and their lateral r, nephridium (kidney); t\ aperture 01 tho
1 ^„„i .. 1 „ v^ ^« Ar. nephridium: c, heart; br, ctenidium (giU-
branches has been de- piJ^e,; pt,:_ pkrabrancUia (=thc osphradium
te<-;ted (30). The his- or ollactory patch); i, glandular lamellae of
. , ^ £ ii. the inner fece of the mantle-skirt ; i), adrectal
tOlOgy 01 the nervous (pnrpuriparous) gland ; (, testis ; vd, vas de-
Rvst^m nf Arnllnwa. ferens; p.pcnls; mc,columellarauscle(muscular
system 01 MOUUSCa pjo^jjJglJspio^tgshell); •>, stomach ;>,liver.
has yet to be sen- y.B. Note the simple snout or rostrum not in-
OUsly inquired into. txovened as a -proboscis."
The alimentary canal of the Azygobranchia presents
little diversity of character, except in so far as the buccal
region is concerned. Salivary glands are present, and in
some canuToroua forma (Dolium) these secrete freejgk
652
MOLLUSCA
[AZTCOBl^AJfCElO
of the animal so as to expose
the organg on its inner face.
a, anuy ; vg, vagina ; g^, adrec-
tal piirpuripaioua gland ; r',
apprtuic of the nuphridimn (kid-
ney); br, etenidium (branchial
plUiiie): fc/, parabranchia( = the
corab-like osphradium or olfac-
tory organ).
phuric acid (as much as two per cent is present in the
uecretion), which assists the animal in boring holes by
means of its rasping tongue through the shells of other
Molluscs upon which it preys. A crop-like dilatation of
the gut and a recurved intestine, embedded in the com-
pact yellowish-brown liver, the ducts of which open into it,
form the rest of the digestive tract and occupy a large
bulk of the visceral hump. The buccal region presents a
pair of sheUy jaws placed laterally upon the lips, and a
wide' range of variation in the form of the denticles of the
lingual ribbon or radula, the nature of which will be un-
derstood by a reference to fig. 9, whilst the systematic list
of families given above shows the particular form of den-
tition characteristic of each division of the order.
The modJ-ficatiou in the form of the snout upon which
thn mouth is placed, leading to the
distinction of " proboscidif erous "
and " rostriferous " Gastropods, re-
quires further notice. The condi-
tion usually spoken of as a " pro-
boscis " appears to be derived from
the condition of a simple rostrum
(having the mouth at its extrem-
ity) by the process of incomplete _
introversion of that simple rostrum. '".^-A. I irvV ^''
There is no reason in the actual „
• c J. .-, 1 T ^1 Fig, 47.— Female of Purpum ?a
Slgnincance Ot tae word why the yiWus removed from its shell
term "proboscis" should be applied f"," manticsidrt cut along it
\ . ., f ^ , left Ime of attachment and
to &" alternately mtroversible and tiu-mtn overto the rieht side
evarsible tube connected with an
animal's body, and yet such is a
very customary use of the term.
The introversible tube may be
completely closed, as in the " i)ro-
boscis" of Nemertean worms, or
it may have a passage in it leading into a non-eversible
oesophagus, as in the present case, and in the case of the
eversible pharynx of the predatory Chaetopod worms. The
diagrams here introduced (fig. 48) are intended to show
certain important distinctions which obtain amongst the
-various "introverts," or intro- and e-versible tubes so fre-
quently met with in animal bodies. Supposing the tube
to be completely introverted and to commence its ever-
eion, we then find that eversion may take place, either
by a forward movement ot the side of the tube near its
attached base, as in the proboscis of the Nemertine worms,
the pharynx of Cha:topod3, and the eye-tentacle of Gastro-
pods, or, by a forward movement of the inverted apex
of the tube, as in the proboscis of the Ehabdocoel Plauar-
ians, and in that of Gastropods here under consideration.
The former case we call " pleurecbolio " (fig. 48, A, B, C,
H, I, K), the latter "acrecboUc" tubes or introverts (fig.
48, p, E, F, G). It is clear that, if we start from the
condition of full eversion of the tube and watch the pro-
cess of introversion, we shall find that the plcurccbolic
variety is introverted by the apes of the tube sinking in-
wards; it may be callod acrembolic, whilst conversely the
acrccbolic tubes are pleurembolic. Further, it is obvious
enough that the process either of introversion or of eversion
Of the tulje may be arrested at any point, by the develop-
wcp.t of fibres connecting the wall of the introverted tube
■with the wall of the body, or mth an axial structure such
as the oesophagus ; on the other hand, the range of move-
ment of the tubular introvert may be unlimited or complete.
The acrembolic proboscis or frontal introvert of the Nemer-
tine worms has a complete range. So has the acrembolic
pharynx of Chstopods, if we consider the organ as ter-
minating at that point where the jaws are placed and the
oesophagus commences. So too the aurembolic eye-tentacle
of the snail has a comjilele range of movement, and also the
pleurembolic proboscis of the Eiabdoccel prostoma. The
introverted rostrum of the Azygobranch Gastropods pre-
sents in contrast to these a limited range of moveipent.
The " introvert " in these Gastropods is not the pharynx as
in the Chsetopod worms, but a pree-oral stmctiue, its apical
limit being formed by the true lips and jaws, T/lulst tho
apical limit of the Ch:Etopod's introvert is formed by the
jaws placed at the junction of pharynx and oesophagus, so
that the Chaatopod's introvert is part of the stomodKum
or fore-gut, whilst that of the Gastropod is e:!:temal to the
alimentary canal altogether, being in front of the mouth,
not behind it, as is tho Chjetopod's. Further, the Gastro-
pod's introvert is pleurembolic (and therefore acrecboUc),
and is limited both in eversion and in introversion j it can-
Fia. 4S. — DU»grania explanatory of the natur* of so-called proboscldes or "intra-
verls." A. Simple introvert completely introverted. B, The same, partially
everted by eversion of the sides, as in the Nemertine proboscis and Gastropod
eye-tentaclc^pleurccbolic. C. Tlie same, fully everted. D, E. A similar
simple introvert in course of eversion by the forward movement, not of ita
sides, but of its apex, iS in the proboscidean Rbabdoccel3=acrecbolic. P.
AcrecboUc (= pleurembolic) introvert, formed by the snout of the proboscidl-
ferous Gastropod, al, alimentary caual ; d, the true mouth, Tlie introvert
is not a simple one v;ith complete range both in eversion and introvereion,
but is arrested in introvoi-sion by the fibrous bands at c, and similarly in
eversion by the fibrous bands at I: 0. The acrecboUc snout of a pivbos-
cidifcroua Gastropod, arrested b'l ■ ' (,■■ virsion by the fibrous band
&. H. The acrembolic (spUmr ..fa Chxtopod fully intro-
verted, ai, alimentary canal ; :l: ", the mouth ; therefore o
to d is storaodtcum, vi'hereas in Ul. i , , ;. , - i tt)n to d is inverted body-
surface. I, Partial eversion ot 11. k, i.„mpKlu eversion otH, (Original,)
not be completely everted owing to the muscular bands
(fig. 43, G), nor can it be fully introverted owing to the bands
(fig. 4S, I') which tie the axial pharynx to the adjacent
wall of the apical part of the introvert. As in all such
intro- and e-versible organs, eversion of tho Gastropod
proboscis is efi'eclcd by pressure communicated by the
muscular body-wall to the liquid contents (blood) of the
body-space, accompanied by the relaxation of the muscles
v.-hich directly pull upon either tho sides or tho apex of
the tubular orgau. The inTcrsion of the proboscis is effected
directly by tho contraction of these muscles. In various
members of the Ajrrgobranchia the mouth-beariug cylinder
is introversible (I'.e , i." n proLoscis) — ■with rare exceptions
these forms have a siphonate mantle-skirt. On the other
hand, many which have a siphonate mantle-skirt are not
provided with an introversible moulh-bcaring cylinder; but
have a simple nou-introversible rostrum, as it has beeni
JUTGOBKANCEIA.]
MOLLUSCA
653
tensed, which, is also the condition presented by the mouth-
, bearing region in nearly all other Gastropoda. One of the
best examples of the introversible mouth-cylinder or pro-
iboscis which can be found is that of the Common VSTielk
'4nd its immediate allies. In fig. 37 the proboscis is seen
in an everted state ; it is only so carried when feeding,
being withdrawn when the animal is at rest. Probably
its use is to enable the animal to introduce its rasping
and licking apparatus into very narrow apertures for the
purpose of feeding, e.g., into a small hole bored in the shell
of another Mollusc.
The foot of the Azygobranchia, unlike the simple mus-
cular disc of the Isopleura and Zygobranchia, is very often
divided into lobes, a fore, middle, and hind lobe (pro-,
meso-, and meta-podium, see figs. 39 and 43). Very usually,
but not universally, the meta-podium carries an operculum.
The division of the foot into lobes is a simple case of that
much greater, elaboration or breaking up into processes and
regions which it undergoes in the class Cephalopoda. Even
among some Gtastropoda (viz., the Opisthobranchia), we
find the lobation of the foot still further carried out by
the development of lateral lobes, the epipodia, whilst there
are many Azygobranchia, on the other hand, in which the
foot has a simple oblong form without any trace of lobes.
The development of the Azygobranchia from the egg has
been followed in several examples, e.g., Paludina, Purpura,
Nassa, Vermetus, Neritina. As in other Molluscan gcoups,
we find a wide variation in the early process of the forma-
tion of the first embryonic cells, and their arrangement as
a Diblastula dependent on the greater or less amount of
food-yelk which is present in the egg-cell when it com-
mences its embryonic changes. In fig. 7, the early stages
of Paludina viuipara are represented. There b but
very little food-material in the egg of this Azygobranch,
and consequently the Diblastula forms by invagination ;
the blastopore or orifice of invagination coincides ■nith the
anus, and never closes entirely. A well-marked Trocho-
Bphere is formed by the development of an equatorial
ciliated band ; and subsequently, by the disproportionate
growth of the lower hemisphere, the Trochosphere becomes
a Veliger. The primitive shell-sac or sheU-gland is well
marked at this stage, and the pharynx is seen as a new
ingrowth (the stomodaeum), about to fuse with and open
into the primitively iavaginated arch-enteron (fig. 7, F).
In other Azygobranchs (and such variations are repre-
sentative for all Mollusca, and not characteristic only of
Azygobranchia), we find that there is a very unequal
division of the egg-cell at the commencement of embryonic
development, as in Nassa (fig. 5). Consequently there is
strictly speaking no invagination (emboly), but an over-
growth (epiboly) of the smaller cells to enclose the larger.
The general features of this process and of the relation of
the blastopore to mouth and anus have been explained
above in treating of the development of Mollusca generally.
In such cases the blastopore may entirely close, and both
mouth and anus develop as new ingrowths (stomodseum
and proctodoeum), whilst, according to the observations of
Bobrotzky, the closed blastopore may coincide in position
with the mouth in some, instances (Nassa, itc), instead of
with the anus. But in these epibolic forms, just as in the
embolic Paludina, the embryo proceeds to develop its cili-
ated band and shell-gland, passing through the earlier con-
dition of a Trochosphere to that of the Veliger. In the
▼eliger stage many Azygobranchia (Purpura, Nassa, (tc.)
exhibit, in the dorsal region behind the head, a contractile
area of the body-wall. This acts as a laF\'al heart, but
ceases to pulsate after a time. Similar rhythmically con-
tractile areas are found on the foot of the embryo Pulmo-
nale Limax and on the yelk-sac (distended foot-surface),
of the Cephalopod Loligo (see fig. 72**).
The history of the shell in the development of Azygo-
branchia (and other Gastropods) is important. Just as
the primitive shell-sac aborts and gives place to a cap-like
or boat^like shell, so in some cases (Marsenia, Krohn) has
this first shell been observed to be shed, and a second shell
of different shape is formed beneath it.
/- detailed treatment of what is known of the histo-
genesis in relation to the cell-layers in these Mollusca would
take us far beyond- the limits of this article, which aims at
exposing only the well-ascertained characteristic features
of the Mollusca and the various subordinate groups. There
is still a great deficiency in our knowledge of the develop-
ment of the Gastropoda, as indeed of all classes of animab.
The development of the gill (ctenidium) as well as of the
renal organ, and details as to the process of torsion of the
visceral hump, are still quite insufficiently known.
One fm ther feature of the development cf the Azygobran-
chia deserves special mention. Many Gastropoda deposit
their eggs, after fertilization,. enclosed in capsules; others, as
Paludina, are viviparous ; others, again, as the Zygobranchia,
agree with the Lamellibranch Conchifcra (the Bivalves) in
having simple exits for the ova without glandular walls,
and therefore discharge their eggs unenclosed in capsules
freely into the sea-water; such unencapsuled eggs are
merely enclosed each in its own delicate chorion. When
egg-capsules are formed they are often of large size, have
tough walls, and in each capsule are several eggs floating
in a viscid fluid. In some cases all the eggs in a capsule
develop ; in other cases one egg only in a capsule (Neri-
tina), or a small proportion (Purpura, Buccinum), advance
in development ; the rest are arrested either after the first
process of cell-division (cleavage) or before that process.
The arrested embryos or eggs are then swallowed and
digested by those in the same capsule which have advanced
in development. The details of this history requiie renewed
study, our present knowledge of it being derived from the
works of Keren and Danielssen, Carpenter and Claparide.
In any case it is clearly the same process in essence as that
of the formation of a vitellogenous gland from part of the
primitive ovary, or of the feeding of an ovarian egg by
the absorption of neighbouring potential eggs ; but here
the period at which the sacrifice of one egg to another
takes place is somewhat late. What it is that determines
the arrest of some eggs and the progressive development
of others in the same capsule is at present unknown.
Section h (of the Azygobranchia).— AOi TANTIA.
Characters. — Azygobranchiate Strcptoneura which havo th9
form and texture of the body adapted to a frce-swTrnniing pelagio
habit. They appear to be derived from holochlamydic foiTES of
Reptant Azygobranchia. The foot takes the form of a swimmin".
organ. Thererrous system and sense-organs (eyes, otocysts, and
osphradi>iTii) are highly developed. The odontopliore also is re-
markably developed, its admedian teeth being mobile, and it serves
as an efficient organ for attacking other pcla.i;ic forms upon which
the Natantia prey. The sexes are distinct as in all Streptoncura ;
and genital ducts and accessory glands and pouches are present as
in all Azygobranchia. The Natantia exhibit a series of modifica-
tion!! of the form and proportions of the visceral mass and foot,
leading from a condition readily comparable with that of a typical
Azygobranch such as RostcUaria, with the three regions of the foot
(pro-, meso-, and meta-podium) strongly marked, and a coiled
visceral hump of the usual proportions, up to a condition in which
the whole body is of a tapering cylindrical shape, the foot a platc-
like vertical fin, and the visceral hump almost completely atrophied.
Three steps of this modification may be distinguished as three sub-
orders, the Ailanlacea, the Carinariacca, and the PUrolrachcacea.
Sub-order 1. — Atlanlacca.
C7iaracfers.— Natantia with a large spirally-wound visceral hump,
covered by a hyaline spiral shell ; mantle-skirt large, overhangms
a well-developed sub-paliial branchial chamber as in A^ygobi-anchia,
to the wall of which is attached tha branchial ctcniJium ; foot
well developed, divisible into a mobile propodiiim, a mcsopodiuni
on which is formed a sucker, and a metapodium which, when the
animtil is expanded, extends backwards beyond the shell and visceral
654
MOLLUSCA
[AZTGOBEANCHlia
the viscera] looo of iha lifataatia ia StrsBtonenror^ Special
to the Natantia is the liigli elaboration of the Ungual
ribbon, and, as an agreement with some of the Opistho-
branchiata Euthyneura but as a difference from the Azygo.
branchia, we find the otocysts closely attached to the cerebral
ganglia. This is, however, less of a difference than it waa
Immp ; npon the cppor surface of the met&podiam h developed an
<iporculum.
Genera : Atlanta, OxyguTJU. Probably here belong the Paljeozoic
fossils BellcTophtm.
Sub-order 2. — Oarinariacea.
Characters. — Visceral hump greatly reduced in relative size ;
shell small, cap-like, hyaline ;
-ctenidium (branchial plume)
projecting from Lbe small sub
pailial chamber ; body cylin
flrical ; of the foot-lobes only
the mesopodjiun is prominent,
provided with a sucker, and
compressed laterally so a.s to
form a vertical plate -Uko fin
projecting from the ventral
surface ; the propodium forms
simply the ventral surface of
the anterior region of the cy-
lindrical body whilst the roe-
tapodium forms its posterior
region.
Genera : Carirutria, Cardio-
poda-
Snb-oi-der 3, — Ptcrotracheacea.
Characters. — Visceral hump
still further reduced, forming
a mere oval sac embedded in
the posterior doi-sal region of
the cylindrical body ; no shell ;
foot as in Carinariacea, excent
that the sucker is absent from
the mesopodium in the females.
Genera : Pterotrachea, Firu- ^'"^ 60.— Carinarto midUtrranea. A, The ammal, B. The shell removed. 0, D, Two Tiews of the shcD of Caidlopoda.
Jffi^gs ^ mouth aud w^ontophore ; 6, cephalic tentacles ; c. eye ; d, the Qn-Iike mesopodium ; d', its sucker ; e, metapomum;
/, Balivary glanda ; \ hoHer of the mantle-e:ip ; i, cienidium (gill-plume) ; m, stomach ; n, inteatijie ; o, anus ; p, liver
Further Jlemarlis on the '' '^'^ eprmgiug from the ventricle ; u, cerebral ganBlion ; i>, pleural and pedal ganglion ; w, testis ; x, \iscenil gnngUoD
,) V..01.-111.. Damin,i.„ . ™ pg[j^_ (From Owen.)
, veaicula seminali.
Natantia Azygobranchia. —
liOgically the Natantia should stand as we have placed them,
viz., as a special branch or section of the Azygobranchia,
related to them somewhat as are the Birds to the Reptiles.
They are time Azygobranchia which have taken to a pelagic
life, and the peculiarities of structure which they exhibit
Fio. i^.—ACtanta (Oxygum) Kemwlrmil (m.ignlBed 20 dlamnt*™). a, month
and odontophoro ; 6, cephalic tentacles ; c, eye ; d, propodium (B) and moao-
podium ; e. metapodium ; / operculum ; It, mantle-chamber ; i, ctenidium
(gill-plume) , k, retracwr mnajlo of foof ; l, optic tentwlp : m, iWmach ; n,
dorsal surlace overhung by the m.intlo.nkirt, the letter Is close to the salivary
filand ; o, rectum and anus ; p, liver ; (/, renal organ (nephridium)!; s, ven-
tricle ; u, the otocyst attached to the cwobia! ganglion ; w, testis ; a:, auricle
of the heart ; y, vesicle on gcuital duct ; b, penis. (From Owen.)
are strictly adaptations of tlie otracture common to them
and the Azygobranchia consequent upon their changed
mode of life. Such adaptations are the transoarency and
colourlessness of the tissues, and the modifications of the
foot, which still shows in Atlanta the form common in
Azygobranchia (compare fig, 49 and fig. 39).
The cylindrical bouy ol t'teroiracheuoea la paralleled by
the slug-like forms of Euthyneura. Spengel baa shown that
at one time supposed to be, for it has been shown by Lacaze
Duthiers, and also by Leydig, that the otocysts of Azygo-
branchia even when lying close upon the pedal ganglion
(as in fig. 21) yet receive their special nerve (which can
sometimes be readily isolated) from the cerebral ganglion (see
fig, 36), Accordingly the difierence is one of position of the
otocyst and not of its nerve-supply. The Natantia are further
remarkable for the high development of their cephalic eyes,
and for the typical character of their osphradium (Spengel'a
olfactory organ). This is a groove, the edges of which are
raised and ciHated, lying near the branchial phuno in
the genera which possess that organ, whilst in Firuloides,
which has no branchial plume, the osphradium occupies a
corresponding position. Beneath the ciliated groove is
Fio. 61. — Pterotmchen mvltca. e
of the snout when retracted :
g, cerebral p.inglion ; ff", plei
stomach ; i
to, osphradii
B from the right side, a, pouch for reception
pericardium ; ph, pharynx ; oc, ceph.ilic eye ;
dal ganglion ; pr, foot (mesopodium) ;
: ml, foot (metapodium) ; s, caudal appen Jage. (After Kefer*
placed an elongated ganglion (olfactory ganglion) connected
by a nerve to the supra-intestinal (therefore the primitively
dextral) ganglion of the long visceral nerve-loop, the strands
of which cross one another, — this being characteristic of
Streptoneura (Spengel).
The Natantia belong to the " nehjgic fauna " occurring
near the surface in the Mediterranean and great oceans in
company with the Ptoropoda, the Siphonophorous Hydrozoa,'
Salpae, Leptocephali, and other specially-modified trans-
parent swimming representatives of various groups of the
animal kingdom. In development they pass through the
typical trocLosphere (mj veliger stages p rovided with bont*
like sheU.
Bfisihobkanchia.] MOLLUSCA
Branch h.—EUTETNEUBA (Spengel, 1881).
Characters. — Gastropoda Anisopleura in which the
visceral loop (the contenninous visceral nerves) does not
share in the torsion of the visceral hvunp, but, being placed
entirely below the intestine, remains straight and untwisted,
'the junction of the visceral cords being below, and not
Fio. 62.— Biino vaMun (Oicmnlt!), ai seen crawling, d, oral lood (compare
with Tetbys, fig. 62, B), possibly a continnation of the epipodia; &, &', cepnalic
tontaclea. (From Owen.)
above, the intestine as it is in Streptonenra. Although
the anus is not brought so far forward by the visceral
torsion as in the Streptonenra, and may §ven by secimdary
growth assume a posterior median position, yet, as fully
developed, an asymmetry has restilted as in the A^ygo-
brancMa, only the original right renal organ, right cteni-
dium (if any), right osphradium, 'right side of the heart,
and right genital ducts being retained. All the Euthy-
neura are hermaphrodite. The lingual ribbon has very
usually numerous fine denticles J— -^ i
undifferentiated into series in ^-^^ ^ — *■
each row. The shell is light
and little calcified; often it is
rot developed in the adiUt,
though present in the embryo. ^^ -
An operculum, often found in d "
the embrro, is never present in P'o- 63.— Tomateiia. h, ahen ; 6,
the adult /except in TomateUa, o"i !«»*; d. foot ;/. operculum.
fig. 53). Many Euthyneura show a tendency to, or a
complete accomplishment of, the suppression of the maTille-
akirt as well as of the shell, also of the ctenidiu.ra, and ac-
quire at the same time a more or less cylindrical (slug-LL^e)
form of body.
The Euthyneura comprise two orders, the Opistho-
branchia and the Pulmonata.
Order 1. — OpistholrancMa.
Marine Euthyneura the more archaic forms of which
have a relatively large foot and a small visceral hiunp,
from the base of which projects on the right side a short
mantle^kirt. The anus is placed in such forms far back
. Fm. 64. — XJmbreHa meSittm'aea, a, mouth ; h, ceplia]
(ctenldlmn). The free edse of the mEntle Is seen Jutt bslow tho matginof
the ahell (compare with Aplyaia, flg. 63). (EVom Owen.)
fceyond the mantle-skirt. In front of the anus, and only
partially covered by the mantle-skirt, is the ctenidium with
its free end turned backwards. The heart lies in front of,
instead of to the side of, the attaclur.ent of the ctenidium,
— .hence Opisthobranchia as opposed to " ProsobranchL*,"
655
which correspond to the' Streptonenra. A shell is possessed
in the adult state by but few Opisthobranchia, but all paa*l
through a veliget larval stage with a nautiloid shell (fig. 60)k,
Many Opisthobranchia have
by a process of atrophy lost
the typical ctenidium and the
mantle-skirt, and have deve-
loped other organs in their
place. As in some Azygo-
braachia, the free margin of
the mantle-skirt is frequently
reflected over the sheU when
a shell exists ; and, as in some
Azygobranchia, broad lateral
outgrowths of the foot (epi-
podia) are often developed,
which, as d oes «o< occur in Azy-
gobranchia, may be thrown
over the shell or naked dorsal ,
surface of the body. ^ ^ , ^ v *v ?.»
rm. • 1. £ • 1 J _ tentacles ; k. penis-sneath. (After
The variety of special deve- Keferstein.)
lopments of structure accom-
panying the atrophy of typical organs in the OpisthobranchiL
and general degeneration of organization is very great, an&
renders their classification difficult. Two sections of the
order may be distinguished, according as the typical
Molluscan mantle-skirt (limbus pallialis) is or is not atro-
phied, and within each section certain sub-orders.
aecUon a.— PALLIA TA {^TecHbrancJiiata, Woodward)— the
typical Molluscan mantlc-skirt or pallium retained.
Sub-order 1. — Ctenidiohranchia,
Characters.— Palliata in which the ctenidium U retained as thj»
branchial organ ; with rare exceptions a delicate shell, which may
be very smaU or completely enclosed by the reflected margin of th»
mantle ; cpipodia (lateral outgrowths of the foot) freq^uently present.
Family 1. — TomcUelHdw.
Genera : Tomautla, lam. (fig. 63) ; Cirmlia, Gray, ic.
Family i.—BuUida.
Genera : Bulla, Lam. (fig. 62) ; Acera, Miiller ; Scaphander,
Montf. ; Bullssa, Lain. ; Doridium, Meckel ; Gastropteron,
Meckel, &c.
Family 3. — Aplysiid^.
(jeneia : Aplysia, Gmelin (the Sea-Hare) (figs. 20, £6, tus.) i
Dolobella, Lam.; Lobiger, Krohn, &c
Family 4. — PlcurohraTjchida;.
Genera : Pleurohratwhus, Cuvier ; Umbrella, Chemnitz (figs. 64,
65); RximcUm, Forbes, iic.
Sub-order 2. — PhyllidiobrancJiia.
Characters. — Palliata in which the ctenidia have atrophied ; mncb
as in Patellidoe among the Zygobranchiate Streptonenra their placo
is taken by laterally- placed lameilse, developed from the inner surfaco
of the bUaterally-disposcd mantle-shirt in two lateral rows.
Family B. — Phyllidiadee.
Genera : Phyllidia, Cuiver ; Pleurophyllidia, Meek, (fig. 67).
Section i.—NON-PALLIATA.
CK«riwfcrj.— The typical MoUuscan mantle-skirt is atrophied in
the adult No shell is present in the adult, though the dorsal
integument may be strengthened by calcareous spicules (Doris). Tha
otocysts are not sessile on the pedal ganglia as m other Gastropoda,
but, a^ in the Natantia Azygobranchia, lie close to the cerebral ganglia.
In one suborder (Pygobranchia) the typical ctenidium appears to
bo retained in a modified form ; in the others special developments
of the body-wall take its place, or no special respiratory processes
exist at all. The general form of the body is slug-like, the foot
and visceral hiimp being coextensive, and a secondary bilateral
symmetry is asserted by the usually median (sometimes right-sided)
dorsal position of the anus on the hinder part of the body.
Sub-order 1. — Pygobranchia.
Characters. —The ctenidium assumes the form of a circlet of pinnate
processes surrounding the median dorsal anus ; a strongly-marked
epipodial fold may occur all round the foot and siinulate a mantle-
skirt (see fig. 62, C, Doris) ; papillae or " cerata " of the dorsal integu-
ment may occur as well as the true ctenidium (fig. 61).
Family 6. — Dm-ididas.
Genera : Boris, L. ; Oortiodoris, Forbes ; Triopa. Johnst. ; j^girtts
Lo'cn : Thecacera, Fleming ; Polycera, Cuvier ; Idalia, Leuck-
art ; AimUa, Loven; Ceraiosoma, Adams i OruhidoriS; Bloin?..
656
MOLLUSCA
BnB-orJer 2.— Cerofonoto.
Charaders. — The typioil MoUu^can ctenidium is not developed ;
■upon the dorsal area ia developed a more or less numerous series of
cylindrical or branched processes (the ccrata) into each of which tho
intestine usually sends a process ; anus dorsal, median, or right-sided.
Family 7. — TrUov^iacUe.
Genera: Tritonia, Cuvier; Scyllma, L.; Tcthys, L. (fig. 62, B);
Deridronot-iis, A. and H. ; Doio^ Oken.
Family S.—SoHrlm.
Genera : Eolis, Cuvier (fig. 62, A) ; Glaums, Forster ; Fiaiua, A.
and H. (Sg. 57); Embldonia, A. and H.; Proctmotus, A. and
H. ; Aitiicpa, A. and H.; Mcrjnma, Loven; Alderia, AHm.^n.
Sub-order 3. — Haplomorpha.
diaraclATS. — No ctenidia, cerata, mantle-skirt, or other processes
of the body-wall ; degenerate forms of email size.
FamJJy O.—PKyllirhcridia.
Gsnera : Phyllirhoe, Peron and Lesnenr (fig. 5S) ; Acura, Adams.
Family 10. — Elysiadaj.
Genera: Eiysia, Risso (fig. 62, D, E) ; Actconia, Qnatroi; Ccnia,
A. and H. ; Liviaponiiaf Johnston ; HJiodope, Kbli.
Fi'Hhc)' Bsmarlcs on the Opisthohranchia. — The Opia-
thobvanchia present the same wide range, of superficial
aDpcaranco as do the Azygobranchiato Streptoneura, forma
Sio. M.— Threo views of Aplysla sp., to vailons conditions of expansion and
retraction. (, anterior cephalic tentacles ; (2, posterior cephalic tentacles ;
c, eyes ; / metapoUiiim ; ep, epipodium ; g, gill-pliune(ctemdium) ; m, mantle-
Sap reflected over tho thin oval shell ; os, s, oriCco formed by the imdosed
border of the reflected mantle-sliirt, allowing the iiiell to show ; jk, tho sper-
matic groove. (After Cuvier.)
carrying well-developed spiral shells gud large mantle-
skirts being included in the group, togedier with flattened
or cylindrical slug-
like forms. But ia
respect of the substi-
tution of other parts
for the mantle-skirt
and for the gill which
the mors degenerate
Opisthohranchia ex-
hibit, this Order
staads alone. Some
Opitithobranchia are
Btrikiiig examples of
degeneiation (some
Haplomoi-pha), hav-
ing none of those re-
gions or processes of .p,„ 67.-Dor»al
the body developed dwiinmtacottoi,
. . 1 T 1* -1 Falllalc Opistbybrancna. o, tno i
Wnicn UlStingUlSn lamoUirormBUb-pallialRiUs, whlch(,ii!iuPatdla)
the archaic MoUusca replace tbo typical Mollus&m ctenidium. (After
, 1. .1 . Kefcrstem.)
from such iiat-wonna
as the Dendroco;! Planarians. Indeed, were it not for their
retention of tho characteristic odontophore we should have
lUtle or no indication that such forms as Phyllirhoe and
[I ventral view of PUur^'hyllU
Olio of the rhyllidiobranchiato
Falllalc Opistbobrancha. 6, tho mouthy Z, tho
I^OPISTBOEEANCHIA.
Limapoctia really Lelocg to the MollD'.ca at oil. The inter-
esting little Rhodove Ve-ranyii, which has no odontophore,
has b;en associated by systematists both with these simpli-
fied Opistl'obranchs and with Rhahdoccel Planarians (89).
In many respects „. „; 7; -
the Sea-Hare (Aply-
sia) of which several
species are known
(some occurring on
the English coast),
serves as a conven-
ient example of tho y_^_ j3._pSsn,>!io? f.cjsafa, t^ce the natnral
fullest development 0I20, a transp::rcnt picciform pc!agic Opistho-
nf tliB nrmnij-a^iATi *i™"ch. Tho iEtcmal organs ore sho-.ra as seen
01 tue Organt^avlOU i,y tmnsmittod light, o, mouth; 5, radnlar sac;
characteristic of c, CEsophagna ; J, stomach ; c', ialtstine ; y, anus :
^. . , , , 1 . ff, g', g", >/", the four lobcj cf the liver; ft, the
(JpiStnobrancriia. he-irt '•auricle and ve^jtricW ; I, the lenal sac (no-
Thewoodcut ('a.!'. 56) Phridimn) ; e; the ciliated communiaition of the
r • 1 ,. 1 renal sac with tiie nenciror.iTn; m, the external
givesafaitnliurepre- opening ofthe renal sac; n, the cerebral ganglion;
<ipnt:fltinnnf tTlPtrrpftt "• ">« ceplialio bentacla; /, the genital pore;
sentaiionoi tUL great, ^^ j,jg ovo- testes: w, the parasitic bydronicdiisa
mobility of the vari- Jfn<5tra,nsnally found atiachcd in this position by
r £,1. 1. J theaboralpoleofitsumbrelia. (After Keferstcin.)
ous parts of the body.
The head is well marked and joined to the body by a some-
what constricted neck. It carries two pairs of cephalio
tentacles and a pair of sessile eyes. The visceral hump is
low and not drawn out into a spire. The foot ia long,
carrying the oblong visceral mass upon it, and projecting
(as metapodium) a little beyond it (/). Latei-ally the
foot gives rise to a pair of mobile fleshy lobes, the epipodia
{ep), which can be thrown up so as to cover in the dorsal
Vio. ^Q,~AixrahuUaia. A single row of teeth of tho radola, (Formula, xls.)
surface of the animal. Such epipodia are common, though
by no means universal, among Opisthohranchia. The
torsion of the visceral hump is not carried out very fuUy,
Fio. flO.-A Vollgcr-Iaria of an Opisthobranch (Polycero). /, foot ; C. opra>
cnlnm; mn, anal paplUs; ry, iry, two portions of ijnabsorbcd nutnti™
™iv „A either- side the intestine. Tho nght olocyst is seen at tho root OJ
I nutritivi
le root 0-
m) show.
-,^m_. .,.„., e. ine ruiiii. tj,in;j3i. lo oci^ «.- t
the foot ' H. Trocho.';i)here of on Opistbobrancb (Plcorobianchidiu-^,
in|:rtgV, tho shell-Bl"»nd or primifive sheU-sac ; y, the cita of he ve urn;
»*: the cJmrccneing stomodKum or owl iiivcEliialion; o(, t.ie lelv otocs..t,
W. rcd-coloiued pinmeat spot C. DiMastu'.r. of ex Opisthobnmch (Potf-
cere) with elongated blastopore ot. (All from Lankesicr.)
the consequence being that the anus has a posterior posi-
tion a little to the right of tho median line above the
metapodium, whilst the branchial chamber formed by the
overhanging mantle-skirt, faces tho right side of tho body
instead of lying well to tho front as in Streptoneura and
as in Pnlmonato Euibyneura. The gill-plume which in
Aplysia ia the typical Jlolluscan ctenidium is seen in fig.
OPISTHOBaANCm A. ]
MOLIiUSUA
657
63 projecting from the branchial sub-pallial space. The
relation of Uie delicate shell to the mantle is peculiar,
since it occupies an oval area upon the visceral hump,
the extent of which is indicated in fig.
56, C, but may be better understood
by a glance at the figures of the allied
genus Umbrella (figs. 54, 55), in which
the margin of the mantle-skirt coin-
cides, just as it does in the Limpet,
with the margin of the shell. But in
Aplysia the mantle is reflected over
the edge of the shell, and grows over
its upper surface so as to completely
enclose it, excepting at the small cen-
tral area s where the naked shell is
exposed. This enclosm-e of the shell
is a permanent development of the
arrangement seen in many Strepto-
neura (c.jf., Pyrula, Ovulum, see figs.
38 and 41), where the border of the
mantle can ba, and usually is, drawn
over the shell, though it is withdrawn _
(as it cannot le in Aplysia) when they p„ ei.-Myce™ crisiaia.
are irritated. From the fact that one of the pygobranchi-
... 'J, i-r £ ate Opisthobranchs (doT'
Aplysia commences its- life as a free- sai view), a, anus; sr,
cwimming Velieer with a nautiloid thectenidiumpecouariy
o°. ,, moaiuea so as to encircle
shell not enclosed m any way by the the anus; (.cephalic ten-
border of the mantie, it is clear that Sulbiaf cSlm "e
the enclosure of the shell in the adult seen ten cinb-uke pro-
1 A J • 1 cessea of the dorsal wall,
IS a secondary process. Accordingly, these are the "cerata"
the sheU of Aplysia must not be con- ruydlXpSin"ilher
founded with a primitive shell in its sub -order of Opistho-
sheU-sac, such as we find realized in ^'t; ^^f^""^^
the shells of Chiton and in the plugs Ge|egtaai-,' after Aider
which form in the remarkable tran-
sitory " shell-sac " or " shell-gland " of Molluscan embryos
Fio. 62. ,
A. Eolis papUlMa (Lin.), dorsal view, a, 6, postetlor and anterior cephalic
tentacles ; c, the dorsal " ceiata " (hence Ceratobranchia).
B. Tctitys lepoTina^ dorsal view, a, the cephalic hood ; b, cephalic tentacles ;
c, neck ; d, genital pore ; c, auoa ; /, Urge cerata ; g, smaller cerata ;
A, margin of the foot
C. i>oris (Actinccytiut) t-ubirculaiiu (Cut,), seen from the pedal snrface. m,
- mouth ; &, margin of the head ; /. sole of the foot ; sp, the mantle-like
. epi podium.
D. S. Dorsal and lateral view of Elytia {AcUeon) rin'dls. tp, epipodial ou^
'"■ ^glDWtha. CA/ter Keferatein.)
Xseefigs 7j 58, and 72***). Ap^^ like other Mollusca,
Vw 34
develops a primitive shell-sac in its trochosphere stage of
development (fig. 68), which disappears and is succeeded
by a nautiloid shell (fig. 60). This forms the nucleus of
the adult shell,
and, as the ani-
mal grows, be-
comes enclosed
by a reflexion of
the mantle-skirt.
In reference to
the possible com-
parison of the
enclosed shell of
Aplysia and its
allies with those
of some Slugs and
of Cuttle-fishes,
the reader is re-
ferred to the para-
graphs dealing
especially with
those Molluscs.
When the shell
of an Aplysia
enCiOSCQ m its ^^^ ^j,,,^ reflected away from the mid-line, o/an-
mantle is pushed tenor cephalic tentacle; b, posterior do.; between a
T^pll fn tliA \off ^^^ ^' ^^^ eyes; c, riglit epipodimn; d, left eplpo-
weu lo tne leit, ^,^^ . ^^ hinder part of Wsceral hump ; Jp, postenor
the sub-pallial extremity of the foot; fa, anterior part of the foot
- K underlying the head : p, the ctenidium (branchial
space is lUlly ex- plnme) ; h, the mantle-skirt tightly spread over the
riOSed as in fiff homy shell and pushed with it towards the left side ;
r^^^ r* ^* i) the spermatic groove ; it, the common genital pore
63, and the van- (male and female) ; /, orifice of the grape-shaped (sup-
«,,(, nT^AY.4-,.i.^(, ^( posed poisonous) gland ; m, the ospnradium (olfac-
OUS apertures OI ,j,jy ^jg^^ „{ Spengel) ; r, outline of part of the renal
the body are seen. ^^ (nephridiom) below tlie surface ; o. external aper-
T, . ■ , ture of the nephridium ; p, anus. (Original.)
Postonoily we
have the anus, in front of this the lobate gill-plume, be-
tween the two (hence corresponding in position to that of
the Azygobranchia) we have the aperture of the renal
organ. In front, near the anterior attachment of the gill-
plume, is the osphradium (olfactory organ) discovered by
Spengel, yellowish in colour, in
the typical position, and overly-
ing an olfactory ganglion with
typical nerve-connexion (see fig.
20). To the right of Spengel's
osphradium is the opening of a
peculiar gland which has, when
dissected 0'\t, the form of a bunch
of grapes ; its secretion is said to
be poisonous. On the under side
of the free edge of the mantle are
situated the numerous small cu-
taneous glands which, in the large
Aplysia camelus (not in other
species), form the purple secretion
which was known to the ancients.
In front of the osphradiimi is the
single genital pore, the aperture _
of the common or hermaphrodite ' 'giands a'nTTucts of Apfysi
duct. From this point there Surtfraibi^S^-'^a^"
stretches forward to the right /. veslcuhi seminalis ; k, open-
.,..,,, ?i ing of the Blbuminiparous gland
side of the head a groove tne info the hermaplirodite duct;
spermatic groove-down which ^^^^f'^'g^i"'^^^"*"-
the spermatic flmd passes. ^^ - - -- ^ -•-
' Fio. 64.— Gonad, and acccssoo'
In
the uterine duct ; . .
other Euthyneura this groove may ^S° ' (Ori^nalT" "^ *'""*'
close up and form a canaL At
its termination by the side of the head is the muscolar
introverted penb. In the hinder part of the foot (not
shown in any of the diagrams) is the opening of a large
mucous-forming gland very often found in the Molluscar.
foot
'XVI. — 83
t{5»
MOLLUSCA
[opisthobeanc/ha.
With regard to internal organization we may commence
with the disposition of the renal organ (nephiidium), the
external opening of which has already been noted. The
position of this opening and other features of the renal
organ have been determined recently by Mr. J. T. Cunning-
ham, Fellow of University College, Oxford, who writes as
follows from Naples, February 1883 : —
"There is considerable ancertainty v/ith respect to the names of
the species of Aplysia. There are two forms which are very common
in the Gulf of Jfaples, and which I have used in studying the ana-
tomy of the renal organ in the genus. One is q"ite black in colour,
and measures when outstretched eight or nine inches in length.
The other is light brown and somewhat smaller, its length usually
not exceeding seven inches. The first is flaccid and sluggish in its
movements, and has not much power of contraction ; its epipodial
Iob«3 are enormously developed and extend far forward aktng the
body ; it gives out when handled an abundance of purple liquid,
which is derived from cutaneous glands situated on the under side
of the free edge of the mantle. In the Zoological Station this form
is known as Ap. leporina ; but according to Blochmann it is iden-
tic-il with A. Camclus of Cuvier. The other species is A. dtpilans ;
it is firm to the touch, and contracts forcibly' when irritated ; the
secretion of the mantle-glands is not abundant, and is milky white
in appearance. The kidney has similar relations in both genera,
and is identical with the organ spoken of by many authors as the
triangulai' gland. Its superficial extent is seen when the folds
covering the shell are cut away and the shell removed ; the external
surface forms a triangle v/ith its base bordering the pericardium and
its apex directed posteriorly and reaching to the left-hand posterior
corner of the shell-chamber. The dorsal surface of the kidney
extends to the left beyond the shell-chamber beneath the skin in
the space between the shell-chamber and the left epipodium.
' ' When the animal is turned on its left-hand side aud the mantle-
chambtr widely opened, the gill being turned over to the left, a
part of the kidney is seen beneath the skin between the attachment
of the gill and the right epipodium (fig. 63). On examination
this is found to be the under surface of the posterior limb of the
fland, the upper surface of which has just been described as Tying
eneath the shell. In the posterior third of this portion, close to
that edge which is adjacent to the base of the gill, is the external
opening (fig. 63, o).
" When the pericardium is cut open from above in au animal
otherwise entire, the anterior face of the kidney is seen forming
the post-erior wall of the pericardial chamber : on the deep edge of
this face, a little to the left of the attachment of the auricle to the
floor of the pericardium, is seen a depression ; this depression con-
tains the opening from the pericardium into the kidney.
"To complete the account of the relations of the organ : the right
anterior corner can be seen superficially in the wall of the mantle-
chamber above the gill. Thus the base of the gill passes in a slant-
ing direction across the right-hand side of the kidney, the posterior
end being dorsal to the ajiex of the gland, aud the anterior end
ventral to the right-hand corner.
" As so great a part of the whole surface of the kidney lies adjacent
to external surfaces of the body, the remaining part which faces
the internal organs is small ; it consists of the left part of the under
surface ; it is level with the floor of the pericardium, and lies over
the globular nias^ formed by the liver and convoluted intestine.
"Mere dissection does not give sufficient evidence concerning such
communications as these of the kidney in Aplysia. I studied the
external opening by taking a series of sections through tlio sur-
rounding region of the gland ; to demonstrate the internal aperture
injected a solution of Berlin blue into the pericardium ; it aid not
fill the whole kidney easily, but ran down into 'he mrt a.ljaccnt to
the base of the gill."
Thus the renal organ of Aply.si.'i is slio\vn to conform to
the Molluscan type. The heurt lying within tlio adjacent
pericardium has the usual form, a single auricle and ven-
tricle. The vascular .system is not extensive, the arteries
soon ending in the well-marked sjiongy tissue which builds
up the muscular foot, epipodia, and dorsal body-\v.iIl.
The alimentary eaiiul commences with the usual buccal
mass ; the lips are cartilciginoas, but not armed with horny
jaw.s, though these arc common in other Opisthobranchs ;
the lingual ribbon is multidtnliculato, and a pair of salivary
glands pour in their secretion. The oesophagus expands
into a curioits gizzard, which is armed internally with large
horny processes, some broad and thick, others spinous, fitted
to act as crushing instruments. From this we pass to a
stomach and a coil of intestine embedded in the lobes of a
voluminous liver ; a cajcum of large size is given olT near
the commencement of the intestine. The liver opona by
two ducts into the digestive tract.
The generative organs lie close to the coil of intestine
and liver, a little to the left side. When dissected out they
appear as represented in fig. S*. The essential reproductive
B
organ or gonad consists of both ovarian and testicular
cells (see fig. 65). It is an ovo-testis. From it passes a
common or hermaphrodite duct, which very soon becomes
entwined in the spire of a gland — the albuminiparous gland.
The latter opens into the common duct at the point x, and
here also is a small diverticulum of the duct y. Passing
on, we find not far from the genital pore a glandular spherical
body (the spermatheca a) opening by means of a longiah
duct into the common duct, and
then we reach the pore (fig. 63,
/!•). Here the female apparatus
terminates. But when the male
secretion of the ovo-testis is
active, the seminal fluid passes
from the genital pore along the
spermatic groove (fig. 63,) to
(;he penis, and is by the aid of
that eversible muscular organ
mtroduted into the genital pore
of a second Aplysia, whence it ^
passes into the spermatheca, there "^
to await the activity of the fe-
male element of the ovo-testis of
this second Aplysia. After an
interval of some days — possibly
weeks — the ova of the second
Aplysia commence to descend
the hermaphrodite duct ; they
become enclosed in a viscid secre- Fio 66- Enttric canal of .f olWta
tinn it thfi nnint whprB tho al P<-TiUo!<i. pA, pharynx ; m, mid-
lion at tne point wnere me aa- p,t, with its hepatic appendages
buminiparous gland 0]x;ns into «, all of which are cot ngimsd ;
the duct intertwined with it ;
and on reaching the point where "<><=''■)
th:- ppcrmathecal duct debouches they are impregnated by
the spermatozoa which escape now from the soennatheca
and meet the ova.
The development of Aplysia from the egg presents many
points of interest from the point of view of comparative
embryology, but in relation to the morphology of th«
Opisthobrancliia it is sufficient to point to the occurrence
of a tiochoaphere and a veligcr ."tage (fig. 60), and of a
shell-gland or juimitive shell-sac (fig. 68, siis), which is suc-
ceeded by a nautiloid shell.
The nervous system of Ajilysia will lie found on com-
parison of fig. 20, which represents it, with our schematic
Mollusc (fig. 1, D) to present but little modification. It is
in fact a nervous system in which the great ganglion-pairs
are well developed and distinct. Tlie Euthjmeurous visceral
loop is long, and presents only one ganglion (in Aplysia
cameliu, but two distinct ganglia joined to one another in
OTtgTBOBRlUCBLL.
Aplytia hybrida of the English coast), placed at its extreme
limit, representing both the right and left visceral ganglia
and the third or abdominal ganglion, which are so often
separately present. The diagram (fig. 20) shows the nerve
connecting this abdomino- y
visceral ganglion with the '^ /
olfactory ganglion of Spen- ^ -^J^,-— ^-ViL *
geL It is also seen to be • ' '*''^^^' r^-^^
connected with a more re-
mote ganglion — the genital. T
Such special irregularities
in the development of gan-
glia upon the visceral loop,
ind on one or more of the
main nerves connected with
it, are, as the figures oi ^^^^^"_c^^^„,^^^^^^^^,f^„^
Molluscan nervous systems i^^^ °^ ^* Ceratonotous opistho-
.1. i' 1 V branchsX showing » tendency to fusion
given m tniS article snow, ot the great gangU*. .i, cerebral, pleu-
ver\- frequent. Our figure f^,' and yireexal ganglia united ; S, pc.
"/ "'-^"'^""- ""^ ^^^^ j^ ganglion; C, buccal gangUon ; /),
n the nervous system of CESophageal ganglion connected with the
Aplysia does not give the Sil ;\"n'S;'eeVS°/r S^SllS
Bmall pair of buccal ganglia tentacles ; ,:, nerve to generative organs;
,. ,*^ . ,, >,i d, pedal nerve : c. pedal conunissnre ; e*,
wniCb are, as in all UlOSSO- Tisceral loop or commissure (rx (From
phorOUS Molluscs, present Gcgenbanr, »fter Bergh.)
upon the nerves passing from the cerebral region to the
»dontophore.
For a comparison ol various Opisthobranchs, Aplysia will
ie found to present a convenient starting-point. It is
one of the more typical Opisthobranchs, that is to say,
it belongs to the section Falliata, but other members of the
Palliata, namely, Bulla and TomateUa (figs. 52 and 53),
are less abnormal than Aplysia in regard to their shells and
the form of the visceral hump. They have naked spirally-
twisted shells which may be concealed from view in the
living animal by the expansion and reflexion of the epipodia.
MOLLUSCA
65&
, otocyst also developing
. „ n
r shell-gland. (From Laukcster.)
but are not enclo.'?ed by the mantle, whil.it TomateUa is
remarkable amongst all Euthyneura for possessing an oper-
culum like that of so many Streptoneura.
The great development of the epipodia seen in Aplysia
is usual in Palliate Opisthobranchs; it occurs also in Elysia
(fig. 62, D) among Non-Palliata ; in Doris it seems prob-
able that the mantle-like fold overhanging the foot is to
be interpreted as epipodium, the mantle-skirt being alto-
gether absent, as shown by the naked position of the gills
and anus on the dorsal surface (figs. 61 and 62, C). The
whole surface of the body becomes greatly modified in
those Non-Palliate forms which have lost, not only the
mantle-skirt and the shell, but also the ctenidium. Many
of these (Ceratonota) have peculiar processes developed
on the dorsal surface (fig. 62, A, B), or retain purely
negative characters (fig. SS, D). The chief modification of
internal organization presented by these forms, as compared
with Aplysia, is found in the condition of the alimentary'
canal The Uver is no longer a compact organ opening
by a pair of ducts into the median digestive tract, but wc
find very numerous hepatic diverticula on a shortened'
axial tract (fig. 66). These diverticula extend usually OU'
into each of the dorsal papillae or " cerata " when these an
present. They are not merely digestive glands, but ari
sufficiently wide to act as receptacles oi food, and in them
the digestion of food proceeds just as in the axial portion
of the canaL A precisely similar modification of the liver
or great digestive gland is found in the Scorpions, where
the axial portion of the digestive canal is short and straight,
and the lateral ducts sufficiently wide to admit food into
the ramifications of the gland there to be digested ; whilst
in the Spiders the gland is reduced to a series of simpk
cseca.
The typical character is retained by the heart, peri-
cardium, and the communicating nephridium or renal organ
in all Opisthobranchs. An interesting example of this L«
furnished by the fish-like transparent Phyllirhoe (fig. 58),
in which it is possible most satisfactorily to study in the
living animal, by means of the microscope, the course o:
the blood-stream, and also the reno-pericardial commtin'
cation. With reference to the existence of pores placing
the vascular system La open communication with the
surrounding water, see the paragraph as to Mollusca gener-
ally. In a form closely allied to Aplysia (PleurobranchUs)
such a pore leading outwards from the branchial vein ha.";
been precisely described by Lacaze Duthiers. No such pore
has been detected in Aplysia. In many of the Non-Palliate
OpLsthobianchs the nervous system presents a concentra-
tion of the ganglia (fig. 67), contrasting greatly with what
we have seen in Aplysia. Not only are the pleural ganglia
fused to the cerebral, but also the visceral to these (see in
further illustration the condition attained by the Pulmonatc
Limnasus, fig. 22), and the visceral loop is astonishingly short
and insignificant (fig. 67, «'). That the parts are rightly thw:
identified is probable from Spengel's observation of the os-
phradium and its nerve-supply in these forms ; the nerve tc
that organ, which is placed somewhat anteriorly — on the dor-
sal surface — being given ofif from the hinder part (visceral) of
the right compound ganglion — the fellow to that marked A in
fig. 67. The Ceratonotous Opisthobranchs, amongst other
specialities of structure, are stated to possess (in some casa?
at any rate) apertures at the apices of the "cerata" or
dorsal papillae, which lead from the exterior into the hepatif
cseca. This requires confirmation. Some amongst them
(Tergipes, Eolis) are also remarkable for possessing
peculiarly modified epidermic cells placed in sacs at thi.
apices of these same papillae, which resemble the " thread
cells " of the Planarian Flatworms and of the Coelentera
The existence of these thread-cells is sufficiently remark
able, seeing that the Non-PaUiate Opisthobranchs resemble
in general form and habit the Planarian worms, many o:
which also possess thread-cells. But it is not conceivable
that theirpresence is an indication of genetic affinity between
the two groups, rather they are instances of homoplasy.
The development of many Opisthobranchia has been
examined — e.g., Aplysia, Pleurobianchidium, Elysia, Poly-
cera, Doris, Tergipes. All pass through trochosphere and
veliger stages, and in all a nautiloid or boat-like shell i".
developed, preceded by a well-marked "shell-gland" (sec figs,
60 and 68). The transition from the free-swimming veliger
larva with its nautiloid shell (fig. 60) to the adult form has
not been properly observed, and many interesting pcnnts as
to the true nature of folds (whether epipodia or mantle or
velum) have yet to be cleared up by a knowledge of such
development in forms like Tethys, Do^i^ Phyllidia, Sn.
660
MOLLUSCA
[pUlMOIfAXA
Afl in other MoUuscan groups, we find even in closely-
allied genera (for instance, in Aplysia and Pleurobran-
chidium, and other genej-a observed by Lankester) the
greatest differences' as to the amount of food-material by
which the egg-shell is encumbered. Some form their
Diblastuia by emboly (fig. 7), others by epiboly (fig. 5) ;
and in the later history of the further development of the
enclosed cells (arch-enteron) very marked variations occur,
in closely-allied forms, due to the influence of a greater or
less abundance of food-material mixed with the protoplasm
of the egg.
Order 2 (of the Euthyneura).— Palmonata.
Characters. — Euthyneurous Anisopleurous Gastropoda,
probably derived from an.;estral forms similar to the
PaUiate Opisthobranchia by adaptation to a terrestrial life.
The ctenidium is" atrophied, and the edge of the mantle-skirt
is fused to the dorsal integument by concrescence, except at
one point which forms the aperture of the mantle-chamber,
thus converted into a nearly closed sac. Air is admitted
to this sac for respiratory and hydrostatic purposes, and it
thus becomes a lung. An operculum is never present ; a
contrast being thus afforded with the operculate Pulmonale
Streptoneura (Cyclostoma, &c.), which differ in other
essential features of structure from the Pulmonata. The
Pulmonata are, like the other Euthyneura, hermaphrodite,
with elaborately-developed copulatory organs and accessory
glands. Like other Euthj-neura, they have very numerous
small denticles on the lingual ribbon. The ancestral
Pulmonata appear to have retained both the right and the
left osphradia (Spengel's olfactory organs), since in some
(Planorbis, Auricularia) we find the single osphradium to
be that of the original left side, whilst in others (Limnsus)
it is that of the original right side.
In some Pulmonata (SnaUs) the foot is extended at right
angles to the visceral hump, which rises from it in the
form of a coil as in Streptoneura ; in others the visceral
hump is not elevated, but is extended with the foot, and-
tbe shell' is small or absent (Slugs).
The Pulracnata are divided into two sub-orders according to the
position of tiie cephalic eyea.
Suh-order 1. — Basommatoplwrei.
Characters.- Eyes placed mediad of the cephalic tentacles at their
base ; the embryonic velar area retained in adult life as a pair of
cephalic lobes (fig. 70, v) ; male and female generative apertures
separate, placed (as is typical in Anisopleura) on the right side of
the neck ; visceral hump well developed, with a well-developed
shell ; aquatid in habit.
Family \.—Limnmidse.
Genera; Idmnsms, Lam. (figs. 3, 4, &c.); Chilinia, Gray; Physa,
Draparn. ; .Ancylm, Geoff. ; Planorbis, Miill., &c.
Family 2. — Auriculide!.
Genera : Auricula^ Lam. ; Conomclus, Lam. : PitJuirella, Wood.
■&c.
Sub-order % — Stylom'incUoplKrfa.
Characters. — Eyes placed on the summit of two hollow tentacles ;
■visceral hump well or not at all developed ; shell large and coiled,
or minute or absent ; almost exclusively torrestriaL
Family 1. — Hclicidaj.
Genera: Helix, L. (Cgs. 69, A; 72*); Vitrina, Draparn. ; Sue-
Hnea, Draparn. ; liulimus, Scopoli ; Achaii'ivi, Lam. ; Pupa,
Lam. ; Clausilia, Drapara., &c.
■Family 2. — Limacida (Slugs).
Goncra : Limax, L." ; IncilaT-ia, Benson ; Arion, Ferussac (fig.
69, D) ; Parmacella, Cuvicrr ; Testaalla, Cuvier (fig. 69, C), &c.
(Family 3. — Oncidiades.
Genera : Oncidium, Bachanui ; Peronia, Blainv. {fig. 72) ;
Vaginulus, Ferussac, tc.
Further Remarke cm Pulmonata. — The land-snails and
^Ugs forming the group Pulmonata are widely distinguished
from a small set of terrestrial Azygobranchia, the Pneumo-
nochlamyda (see above), at one time associated with them
on account of their mantle-chamber being converted, as in
Pulmonata, into a lung, and the ctenidium or branchial
plume aborted. The Pneumonochlamyda (represented in
England by the common genus Cyclostoma) have a twisted
Fig. 69.— a series of Stylommatophorous PulinoData, showing tranaitkjoal foma
betn'eeD snail and slug,
A. Kelix pomatia (from Keferstein).
B. Heticophania brevipes (from Keferstein, after Pfeiffer).
0. Ttstacella haliotidea (from Keferstein).
D. Avion aler, the great Black Slug (from Keferstein).
a, SheU in A, B, C, shell-sac (closed) In D ; t, orifice leading Into ths
subpallial chamber Gung).
visceral nerve-loop, an operculum on the foot, a complex
rhipidoglossate or tsenioglossate radula, and are of distinct
sexes ; they are, in fact, Azygobranchiate Streptoneura.
The Pulmonata have a straight visceral nerve-loop, never
an operculum (even in tiie embryo), and a multidenticidata
Via. 70.— A, B, C, Three Tiews of Liimiarus etayntdls, in order to show tllft
persistence of the larval velar area v, as the cLrcum-oral lobM of the aduJt.
m, mouth ; /. foot ; v, velar area, tho margin v corresnondirg rilh tli«
ciliated band which dcmarcatos the velar an^ft or velum of the smbryo Gas-
tropod (see tig. 4, D, B, F, H, I, v). (Original.)
radu]fl,the teeth being equi-formal; and they are hermaphro-
dite. Some Pulmonata (Limn^us, &c.) live in fresh-waters
although breathing air. The remarkable discovery has
been made that in deep lakes such Limmei do not breathe
air, but admit water to tho lung-sac and live at the bottom.
The lung-sac serves undoubtedly as a hydrostatic apparatus
in the aquatic Pulmonata, as well as assisting respiration.
It is not improbable that hero, and in other air-breathing
animals, the hydrostatic function waa the primary oae, and
the respiratory a later deyelopjnent.
•.'JONATA.]
MOLLUSCA
661
Tlis same general range of body-form is sliown in Pul-
monata as in the Natant Azygobrancliia and in the Opit-
thobranchia ; at one extreme we hare Snails with coUed
visceral hump, at the other cylindrical or flattened Slugs
(see fig. 69). Limpet-like forms are also
found (fig. 71, Ancylus). The foot is al-
ways simple, with its flat crawling surface
extending from end to end, but in the
embryo Limnaeus (fig. 4, H) it shows a
bilobed character, which leads on to the
condition characteristic of Pteropoda. ^'rMiiu'^T''MMi'
The adaptation of the Pulmonata to ter- form aiiuatic pui.
restrial life has entailed little modification "°'^'*-
of the internal organization. The vascular system appears
to be more complete in them than in other Gastropoda,
fine vessels and even capillaries being present in place of
lacunae, in which arteries and veins find theii' meeting-
point. The subject has not, however, been investigated
by the proper methods of recent histology, and our know-
ledge of it, as of the vascular system of Molluscs generally,
is most unsatisfactory. In one genus (Planorbis) the
plasma of the blood is coloured red by hemoglobin, this
being the only instance of the pre-
sence of this body in the blood of
GlossopBorous Mollusca, though it
occurs in corpuscles in the blood
of the bivalves Area and Solen
(Lankestcr, 31).
The generative apparatus of the ^j
Snail (Helix) may serve as an ex-
ample of the hermaphrodite appa-
ratus common to the Pulmonata
and Opisthobranchia (fig. 72*).
From the ovo- testis, which lies
near the apex of the visceral coil,
a common hermaphrodite duct v.e
proceeds, which receives the duct
of the compact white albumini-
parous gland E.d., and then be-
comes much enlarged, the addi-
tional width being due to the
development of glandular folds,
which are regarded as forming a
uterus u. Where these folds cease
the conmion duct splits into two
portions, a male and a female. fio.72«.— HermaDhrcxuterepro-
The male duct v.d becomes fleshy Sn^au^KS^).^
ovo-testis : tJ.e, hermaphro-
dite duct ; E.d,, albmninipar.
oiLt glaud; w, uterine dilata-
tion of the hcnnaphrxjdite
duct ; d, digitate accessory
ids on the female duct ;
calciferous gland or dart-
3ao on the female duct ; B.f,
spermatheca or receptacle of
the sperm in copulation, open-
and muscular near its termination
at the genital pore, forming the
penis p. Attached to it is a diver-
ticulum Jl., in which the sperraa- gland's
tozoa which have descended from
the ovo-testis are stored and mo-
delled into sperm ropes or sperma-
tophores. The female portion of
the duct is more complex. Soon
after quitting the uterus it is joined by a long duct leading
from a glandular sac, the spermatheca (S/). In this duct
and sac the spennatophores received in copulation from
another snail are lodged. In Selix horteneis the speiin&'
g into the female duct ; v.d,
male duct (vas defe«s»s) ; p,
penis ; fl., Cagellum.
theca is simple. In other species of Helix a second duct
(as large in ffelix aspersa as the chief one) is givui off from
the spermathecal duct, and in the natural state is closely
adherent to the wall of the uterus. This second duct has
normally no spermathecal gland at its termination, which
is simple and blunt. But in rare cases in Heluc aspena a
second spermatheca is found at the end of this second duct.
Tracing the widening female duct onwards we now come
to the openings of the digitate accessory glands d, d, which
probably assist in the formation of the egg-capsule. Close
to them is the remarkable dart-sac ps, a thick-walled sac,
in the lumen of which a crystalline four-fluted rod or dart
consisting of carbonate of lime is found. It is supposed
to act in some way as a stimulant in copulation, but pos-
sibly has to do with the calcareous covering of the egg-
capsule. Other Pulmonata exhibit variations of secondary
importance in the details of this hermaphrodite apparatus.
The nervous system of Helix is not favourable as an
example on account of the fusion of the ganglia to form
an almost uniform ring of nervous matter around the
cesophagus. The Pond-Snail (Limnseus) furnishes, on the
other hand, a very beautiful case of distinct ganglia and
connecting cords (fig. 22). The demonstration which it
aftbrds of the extreme shortening of the Euthyneurous vis-
ceral nerve-loop is most instructive and valuable for com-
parison with and explanation of the condition of the nervous
centres in Cephalopoda, as also of some Opisthobranchia.
The figure (fig. 22) is sufiSciently described in the letter-
press attached to it ; the pair of buccal gangUa joined by
the connectives to the cerebrals are, as in most of our figures,
omitted. Here we need only further draw attention to the
osphradium, discovered by Lacaze Duthiers (32), and shown
by Spengel to agree in its innervation with that organ in all
other Gfastropoda. On accoimt of the shortness of the
visceral loop and the proximity of the right visceral
ganglion to the oesophageal nerve-ring, the nerve to the
osphradium and olfactory ganglion is very long. The posi-
tion of the osphradium con-esponds more or less closely
with that of the vanished right ctenidium, with which it is
normally associated. In HeUx and Limax the osphradium
has not been described, and possibly its discovery might
clear up the doubts which have been raised as to the nature
of the mantle-chamber of those genera. In Planorbis, which
is dexiotropic (as are a few other genera or exceptional
varieties of various Anisopleurous Gastropods) instead of
being leiotropic, the osphradium is on the left side, and
receives its nerve from the left visceral ganglion, the whole
series of unilateral organs being reversed. This is, as might
be expected, what is found to be the case in all " reversed "
Gastropods. It is also the case in the Puimonate Auricula,
which is leiotropic.
The shell of the Pulmonata, though always light and
delicate, is in many cases a well-developed spiral " house,"
into which the creature can withdraw itself ; and, although
the foot possesses no operculum, yet in Helix the aperture
of the shell is closed in the winter by a complete lid, the
"hybernaculum," more or less calcareous in nature, which
is secreted by the foot. In ClausiHa a peculiar modifica^
tion of this lid exists permanently in the adult, attached
by an elastic stalk to the mouth of the shell, and known as
the " clausilium." In Ijimnaeus the permanent shell is
preceded in the embryo by a weU-marked shell-gland or
primitive shell-sac (fig. 72***), at one time supposed to be
the developing anus, but shown by Lankester to be identical
with the " shell-gland " discovered by him in other Mol-
lusca (Pisidium, Pleurobranchidium, Neritina, ic). As in
other Gastropoda Anisopleura, this shell-sac may abnorm-
ally develop a plug of chitonous matter, but normally it
flattens out and disappears, whilst the cap-like rudiment jf
the permanent shell is shed out from the dome-like surfact
662
MOLLUSCA
[POLMONATA.
of the yiaceral hump, in the centre of which the shell-sac
existed for a brief period.
In Clausilia, according to the observations of Gcgenbairr,
the primitive shell-sac does not flatten out and disappear,
but takes the form of a flattened closed sac. Within this
closed sac a plate of calcareous matter is developed, and
after a time the upper wall ci the sac disappears, and the
calcareous plate continues to grow as the nucleus of the
permanent shell In the slug Testacella (fig. 69, C) the
shell-plate never attains a large size, though naked. In
other slugs, namely, Limax and Arion, the shell-sac remains
permanently closed over the shell-plate, which in the latter
genus consists of a granular mass of carbonate of lime.
The permanence of the primitive shell-sac in these slugs is
a point of considerable interest. It is clear enough that
the sac is of a diflfercnt origin from that of Aplysia (described
jn the section treating of Opisthobranchia), being primitive
instead of secondary. It seems probable that it is identical
with one of the open sacs in which each shell-plate of a
Chiton is formed, and the series of plate-like imbrications
■which are placed^ behind the single shell-sao on the dorsum
of the curious slug, Plectrophorus, suggest the possibility
of the formation of a series of sheU-sacs on the back of
that animal similar to those which we find in Chiton.
Whether the closed primitive shell-sac of the slugs (and
with it the transient embryonic shell-gland of all other
MoUusca) is precisely the same thing as the closed sac in
which tt? calcareous pea or shell of the Cephalopod Sepia
Fia 72**. — Coraparative dlaeranu of . ,
embryo Cuttle-fish, Loligo (right), gh, internal eYieii ; pfc, e _
organ (Stlobcl'a canal) In Umax ; ml, edge of the mantle-Sap In Loligo ; op,
cephalic eye ; t, cephalic tentacle ; m, position of the mouth ; Ft, tlie foot ;
Fv, the hinder part of the foot drawn out to form the funnel of Loligo ; coti,
the contractile yelk-eac or hernia-Uke protnialon of the mid-region of the foot,
correaponding to the line of closure of the blastopore in LimnEeua. N.B. —
The blastopore in the embryo of Loligo, which, like that of a bird, is much
distorted by excess of food-yelk, docs doae at the extremity of the yeU£-sao
«D». (Original)
and its allies is formed, is a further question, which 'we
shall consider when dealing with the Cephalopoda. It
is important here to note that Clausilia fumiiihes us
with an exceptional instance of the contimtily of the shell
or secreted product of the primitive shell-sac with the
adult shelL In most other Molluaca (Axiisopleurous
Gastropods, Pteropods, and Conchifera) there is a want of
such continuity ; the primitive shell-sac contributes no
factor to the permanent shell, or only a very minute knob-
Uke particle (Neritina and Paludina). It flattens out and
disappears before the work of forming the pennancat shell
commences. And just as there is a break at this stage,
DO (as observed by Krohn in Marsenia = Echiuospira) there
may be a break at a later stage, the nautiloid shell formed
on the larva being cast, and a new shell of a different fonii
being formed afresh on the surface of the visceral hiunp.
It is, then, in this sense that we may speak of primary,
secondary, and tertiary shells in MoUusca, recognizing the
fact that they may be merely phases fused by continuity
of growth so as to form but one shell, or that in other
cases they may be presented to us as separate individual
things, in virtue of the non-development of the later phases.
or in virtue of sudden changes in the activity of the mantle-
surface causing the shedding or disappearance of one phase
of shell-formation before a later one i» entered upon.
The development of the aquatic Pulmonata from the
egg oflers considerable facilities for. study, and that of
LimiuEus has been elucidated by Lank&ter, whilst Eabl
has with remarkable skill applied the method of sections
to the study of the minute embryos of Planorbis. The
chief features in the development of Limn*us are exhibited
in the woodcuts (figs. 3, 4, and 72***). There \s not a
very large amount of food-material present in the egg of
this snail, and accordingly the cells 'resulting from division
are not so unequal as in many other cases. The four cells
first formed are of equal size, and then four smaller cells
are formed by division of these four so as to lie at
one end of the first four (the pole corresponding to
that at which the " directive coi-puscles " dc are extruded
and remain). The smaller cells now divide and spread
over the four larger cells (fig. 3) ; at the same time a space
Pio. 72'*^-— Embryo otLimnrnva sUignalU, at a stage when the TTWbo#pher«
is developing foot and shell-gland and becoming a Vellger, seen as a transparent
object under slight pressure, ph, pharynx (stomodEeal invagination) ; v, v,
the ciliated band marking out the velum ; 715, cerebral nerve-ganglion ; Tt,
Stlebel's canal (left sldeX probably an cvaneacent embryonic nepnridinm ; r^
the primitive shell-sac or shell-gland ; pi, the rectal peduncle or pedicle of
invagination, its attachment to the ectoderm Is coincident with the nmdmost
extremity of the elongated blastopore of fig. S, 0 ; tye, mesoblaaUc (skeleto-
trophic and musicular) cells investing gi, the bilobed arch-enteron or lateral
vesicles of invagiuated endoderm, wUicll will develop into liver ; /, the foot.
(Orisinol.)
— the cleavage cavity or blastocoel — forms in the centre
of the mulberry-like mass. Then the large cells recom-
mence the process of division and sink into the hollow
of the sphere, leaving an elongated groove, the blastopore,
on the surface (fig. 3, C, and fig, 4, G). The invaginated
cells (derived from the division of the four big ceUs) form
the endoderm or arch-entcron ; the outer cells are the ecto-
derm. The blastopore now closes along the middle part of
its course, which coincides in position with the future "foot"
One end of the blastopore becomes nearly closed, and an
ingrowth of ectoderm takes place around it to iorm the
stomodoeum or fore-gut and moutL The other extreme
end closes, but the invaginated endoderm cells remain in
continuity vntii this extremity of the blastopore, and form
the "rectal peduncle" or "pedicle of invagination" of
Lankester (see also the account and figures (fig. 151, A) of
the develojiment of the bivalve Pisidium), although the
endoderm cells retain no contact with the middle rtuion
of the now closed-up blastopore. The anal opening forms
at a late period by a very short ingrowth or proctodseum
coinciding with the blind termination of the rectal peduncle
(fig. 73*** pi).
The body-cavity and the muscular, fibrous, and vascukr
tissues are traced partly to two symmetricaHy-dispoaed
BCAPHOPODiLj
M(JLLUSCA
669
"mesoblasts," which bnd off from the isTaginatcd stfch-
enleron, partly to cells derived from the ectoderm, which
at a very early stage is connected by long processes with
the invaginated endoderm, as shown in fig. 3, D. The ex-
ternal form of the embryo goes through ths same changes
as in other Qastropods, and is not, as was held previously
to Lankester's observations, exceptional. When the middle
and hinder regions of the blastopore are closing in, an
equatorial ridge of ciliated cells is formed, converting the
embryo into a typical " Trochosphere " (fig. 4, E, F).
The foot now protrudes below the mouth (fig. 4), and the
post-oral hemispkereof the Trochosphere grows more rapidly
than the anterior or velar area. The young foot shows a
bilobed form (fig. 4, D, /). Within the velar area the eyes
and the cephalic tentacles commence to rise up (fig. 4, D, <),
and on the surface of the post-oral region is formed a cap-
like shell and an encircling ridge, which gradually increases
in prominence and becomes the freely depending mantle-
skirt. The outline of the velar area becomes strongly
emarginated and can be traced through the more mature
embryos to the cephalic lobes or labial processes of the
adult Limnaeus (fig. 70).
This permanence of the distinction of the part known
as the velar area through embryonic life to the adult state
is exceptional among Mollusca, and is therefore a point of
especial interest in Limnasus. None of the figures of
adult Limnaeus in recent works on Zoology show properly
the form of the head and these velar lobes, and accordingly
the figures here given have been specially sketched for the
present article. The increase of the visceral dome, its
spiral twisting, and the gradual closure of the space over-
hung by the mantle-skirt so as to convert it into a lung-sac
with a small contractile aperture, belong to stages in the
development later than any represented in our figures.
We may now revert briefly to the internal organization
at a period when the Trochosphere is beginning to show a
prominent foot growing out from the area where the mid-
region of the elongated blastopore was situated, and having
therefore at one end of it the mouth and at the other the
anus. Fig. 72*** represents such an embryo under slight
compression as seen by transmitted light. The ciliated
band of the left side of the velar area is indicated by a
line extending from t) to w ; the foot/ is seen between the
pharynx ph and the pedicle of invagination pi. The mass
of the arch-enteron or invaginated endodermal sac has
taken on a bilobed form (compare Pisidinm, fig. 151), and
its cells are swollen {gs and tge). This bilobed sac becomes
entirely the liver in the adult ; the intestine and stomach
are formed from the pedicle of invagination, whilst the
pharynx, oesophagus, and crop form from the stomodaeal
invagination ph. To the right (in the figure) of the
rectal peduncle is seen the deeply invaginated shell-gland
n, with a secretion sh protruding from it. The sheU-gland
is destined in Limnaeus to become very rapidly stretched
out, and to disappear. Farther up, within the velar area,
the rudiments of the cerebral nerve-ganglion ng are seen
separating from the ectoderm. A remarkable cord of cells
having a position just below the integument occurs on each
side of the head. In the figure the cord of the left side is
seen, marked re. This paired organ consists of a string of
cells which are perforated by a duct. The opening of the
duct at either end is not known. Such cannulated cells
are characteristic of the nephridia of many worms, and it
is held that the organs thus formed in the embryo Limnaous
are embryonic nephridia. The most important fact about
them is that they disappear, and are in no way connected
with the typical nephridium of the adult. In reference
to their first observer they are conveniently called "Stiebel'^
canals." Other Pulmonata possess, when embryos, Stiebel's
canals in a more folly-developed state, for instance, the
common sing Limax (fig. 72**, pic). Here too they disap-
pear during embryonic life. FurUier knowledge concern-
ing them is greatly needed. It is not clear whether there
is anything equivalent to them in the embryos of marine
Gastropoda or other Mollusca, the ectodermal cells called
" embryonic renal organs" in some Gastropod embryos hav-
ing only a remote resemblance to them. The three pairs
of transient embryonic nephridia of the medicinal leech,
the ciliated cephalic pits of Nemertines, and the anterior
nephridia of Gfephyneans, all suggest themselves for com-
parison with these enigmatical canals.
Marine Pvlmonata. — Whilst the Pulmonata are essen-
tially a terrestrial and fresh-water group, there is one
genus of slug-like Pulmonates which frequent the sea-
coast (Peronia, fig. 72), whilst their immediate congeners
(Onchidium) are foimd in marshes of brackish water. Sem-
per (33) has shown that these slugs have, in addition to
the usual pair of cephalic eyes, a number of eyes developed
upon the dorsal integument. These dorsal eyes are very
perfect in elaboration, possessing lens, retinal nerve-end
cells, retinal pigment, and optic nerve. Curiously enough,
however, they difi'er from the cephalic MoUuscan eye (for
an account of which see fig. 118) in the fact that, as in
the vertebrate eye, the filaments of the optic nerve pene-
trate the retina, and are connected with the surfaces of the
nerve-end ceUs nearer the lens instead of with the opposite
end. The significance of this arrangement is not known,
but it is important to note, as shown by Hensen, Hickson,
and oiihers, that in the bivalves Pecten and Spondylus,
which also have eyes upon the mantle quite distinct from
typical cephalic eyes, there is the same relationship as in
Onchidiadae of the optic nerve to the retinal cells (fig. 145).
In both Onchidiads and Pecten the pallial eyes have prob-
ably been developed by the modification of tentacles, such
as coexist in an unmodified form with the eyes. The
Onchidiadas are, according to Semper, pursued as food
by the leaping fish Periophthalmus, and the dorsal eyes
are of especial value to them in aiding ■ them to escape
from this enemy.
Class n.— SCAPHOPODA.
Characters. — Molliisca Glossophora with the foot adapted
to a BiTREOWTNG life in sand (figs. 73, 74, /). The body,
Fio. 73.— PejitoJium vulgare, Da C. (afler Lacaie Duthiers). . A. Ventral ri«^
of the aDJinal removed from its shell. B. Dorsal view of the same. C. Lato-
ral view of the same. D. The shell in section. E. Surface view of the sheH
with gill-tentacles eiserted aa in life, a, mantle ; a', longitudinal muscle ;
o", fnnge- surrounding the anterior opening of the mantle-chamber ; a .the
posterior appendix of the mantle ; b, anterior circular muscle of the mantie ;
V, post«rior do. ; c, c", longitudinal muscle of mantle ; e, liver ; / gonad ; 1-,
buccal mas3(8howing through the mantle); o, left nephridium ; i-, club-shapcj
extremity of tlie foot ; w, Iff, longitudinal blood-sinua of the mjmtle.
and to a much greater extent the mantle-skirt and the foot
are elongated along the primitive antero-posterior (oro-a<ial
664
MOLLUSCA
[cephalopoda.
axis, and retain, both externally and in the disposition of
internal organs, the archi-Molluscaji BiLATEEAi symmetey.
The margins of the mantle-skirt of opposite sides (right
and left) meet below the foot and fuse by concrescence ;
only a small extent in front and a small extent behind of
the mantle-margin is left unfused. Thus a cyldtoeical
FOEM is attained by the mantle, and on its surface a tubu-
lar shell (incomplete along the ventral line in the youngest
stages) is secreted (fig. 73, D). ' The foot is greatly elon-
gated, and can be protruded from the anterior mantle-
aperture. It has a characteristic clavate form (fig. 74, /).
The pair of typical ctenidla are symmetrically dove-
loped in the form of numerous eill-filaments (fig. 74, A, g)
margins (a) reflected so as to expose the foot, snout, and glils. B. Lateral
view wth organs showing as thouch by transparency. C. Similar lateral
view to show the number and position of the nei-ve-ganglia and cords, a,
the mantle-skirt ; 6, anterior free margin of the same ; c, hinder extension of
the mantle-skirt ; d, the appendix of the mantle-skirt separated by a valve
ft-ora the peri-anal portion of the snb-pallial chamber, h ; c, the snout or oral
process ; / the foot ; g, the ctenidial filaments ; A, the peri-anal part of the
BUb-pallial chamber ; i, the peri-oral p.irt of the same chamber ; if, the anus ;
/, the left nephridium ; m, the mouth surrounded by pinnate tentacles ; n,
the buccal mass and odontophore ; o, oesopliag:us ; p, the left lobe of the
liver; f).p, pedal ganglion-pair; g.c, cerebiat ganglion-pair; g.pl, pleural
ganglion-pair; p.r, visceral ganglion-pair. Possibly further research will
show that g.pl is the typical visceral g,~nglion-pair, and that ?.v is a pair of
olfactory ganglia placed on the visceral loop as in the Lipocephala according
to SpengeL
placed at the base of the cylindrical cephalic prominence
or snout (fig. 74, e). A pair of nepheldia (fig. 74, .') are
present, opening near the anus (fig. 74, h). The right
serves as a genital duct, the left is apparently renal in
function. The livee (p) is large and bilobed, the lobes
divided into parallel lobules. The nekve-gakgua are
present (fig. 74, C!) as well-marked cerebral, pleural, pedal,
and visceral jxiir." the tyjiical pleural pair being closely
joined to the ceroljral. The visceral loop or commissure is
tmtwisted, that is to say, the Scaphopoda are euthyneup.-
ous. Heaet and distinct vessels are not developed ; a
colourless blood is contained in the sinuses and networks
formed by the body-cavity. The gon^ld.s are either male
or female, the sexes being distinct.
The embyro is remarkable for ' developing five ciliStSd
rings posterior to the ciliated ring and tuft characteristic
of the trochosphero larval condition of Molluscs generally.
These rings are comparable to those of the larva of Pneu-
modermon (fig. 84), and like them disappear.
The class Scaphopoda is not divisible into orders or
families. It contains only three genera : Dentalium, L. (figs.
73, 74) ; Siphonodentalium, Sars. ; and Entalium, Dfr.
They inhabit exclusively the sand on the sea-coast ir
depths of from 10 to 100 fathom
It is worthy of remark that the Scaphopoda constitute
among the Glossophora a parallel to the sand-boring forms
so common among the Lipocephala (such as Solen and Mya).
This parallelism is seen in the special mode of elongation
of the body, in the form of the foot, and in the tubular
form of the mantle brought about by the concrescence of
its ventral margins, as in the Lipocephala mentioned.
The cylindrical shell of Dentalium is also comparable to
the two semi-cylindrical valves of the shell of Solen ; or,
better, to the tubular shell of .Aspergillum and Teredo.
Nevertheless, it is necessary to consider the Scaphopoda as
standing far apart from the Lipocephala, and as having no
special genetic but only a homoplastic relationship to them,
in consequence of their possessing a well-developed odonto-
phore, the characteristic organ of the Glossophora nevei
possessed by any Lipocephala.
Class m.— CEPHALOPODA.
, Characters. — Mollusca Glossophora with the foot prim-
arily adapted to a peee-swiiimln"o mode of life. The
archi-MolIuscan bilatfjcal sysimetev predominates both
in the external and internal organs generally, though in
many cases (especially the smaller forms) a one-sided dis-
placement of primitively median organs and a suppression
of one of the primitively paired organs is to be noted.
An ANTEKiflE, MEDIAN, and POSTEEiOE regiori of the
foot can be distinguished (fig. 75, (4), (5), (6)), corre-
sponding to but probably not derived from the pro-, meso-.
a \
(3)
(5) /^ "•^ i^^(6)
Fio. 75.— Diagrams of a series of Molluscs to show the form of the foot ond ita
regions, and the Kil;!tion of tlic visceral hump to the antero-posterior untl
doi-so-vcntral axes, (ii '. > i * i i^ A I.jimellibranch. (3) An AulsopleuH
ouB Gastropod. (-1) .\ i - Ptcropod. (5) A GyTOuosomatous
Ptcropod. (6) A Si I ill : ! ' A, P, an tero- posterior horizontal
axis: D, V, doreo-vrnii.;! . 1 ; M ii . s at right nnglps to A, P; o, raoutJi ;
a anna; um, cdue of tlu^ m.uii!. m-hL or flap; yp, sub-pallial chamtteroi
space ; /,-fore-loot ; iti/, uudCojC ; /i/, hind-foot ; *r, cepkvlio eyes ; erf, Cfintro-
doraal point (in 0 only).
and meta-podium of Gastropoda. The fore-foot invariably
has the HEAD MKROED into it, and grows up on each sid«
(right and left) of that part so as to surround the mouth,
the two upgrowths of the fore-foof meeting oit the dorsal
aspect of the snout, — whence the name Cephalopoda. In
tbc more typical forms of both branches of the class, the
pori^oral portion of the foot is drawn out into paired arm-
PTKEOPODA.]
MOLLUSCA
665
like processes, either very short and conical (Clio, Eurybia),
or lengthy (Pneumodermon, Octopus) ; these may be beset
with suckers or hooks, or both. The mid-foot (fig. 75, nf)
is expanded into a pair of muscular lobes right and left,
which either are used for striking the water like the wings
of a butterfly (Pteropoda), or are bent round towards one
another so that their free margins meet and constitute a
short tube, — the siphon or funnel (Siphonopoda). The hind
foot is either very small or absent.
A distinctive featuie of the Cephalopoda is the absence
of anything like the toesion of the visceral mass seen in
the Anisopleurous Gastropoda, although as an exception
this torsion occurs in one family (the Limacinidse).
The ANUS, although it may be a little displaced from
the median line, is (except in Limacinida;) approximately
median and posterior. The mantle-skirt may be aborted
(Gymnosomatous Pteropoda) ; when present it is deeply
produced posteriorly, forming a large sub-pallial chamber
around the anus. As in our schematic Mollusc, by the side
of the anus are placed the single or paired apertures of the
KEPHRroiA, the GENlTAt, APERTUTvES (paired only in Nau-
.tilus, in female Octopoda, female Ommastrephes, and male
Eledone), and the paired ctenidia (absent in all Pteropoda).
The VISCERAL HUMP or dome b elevated, and may be very
much elongated (see fig. 75, (4), (5), (6)) in a direction
almost at right angles to the primary horizontal axis (A, P
in fig. 75) of the foot.
A SEELL is frequently, but not invariably, secreted on
the visceral hump and mantle-skirt of Cephalopoda ; but
there are both Pteropoda and Siphonopoda devoid of any
shell. The shell is usually light in substance or lightened
by air-chambers in correlation with the free-swimming
habits of the Cephalopoda. It may be external, when it is
box-like or boat-like, or internal, when it is plate-like. Very
numerous minute pigmented sacs capable of expansion and
contraction, and known as CHP.OMATOPHor.!:.?, are usually
present in the integument in both branches of the class. The
GONADS of both sexes are developed in one individual in some
Cephalopoda (Pteropoda), in others the sexes are separate.
Sense-oroans, especially the cephalic eyes and the oto-
cysts, are veiy highly developed in the higher Cephalopoda.
The o.sphradia have the typical form and position in the
lower forms, but appear to be more or less completely
replaced by other olfactory organs in the higher. The
normal NEEVE-GANCLLi are present, but the connectives are
shortened, and the ganglia concentrated and fused in the
cephalic region. Large special ganglia (optic, stellate, and
supra-buccal) ai-e developed in the higher forms (Siphono-
poda). *
The Cephalopoda exhibit a greater range from low to
high organization than any other Molluscan class, and hence
they are difficult to characterize in regard to several groups
of organs ; but they are definitely held together by the
existence in all of the encroachment of the fore-foot so as
Flo. 76.— 5|>iriaZi5 Tmlinwid**, Bool., one of the Limactnlds enlarged (from
Owenl C C, pteropodial lobes of the mid-foot ; St opoxculoia earned on the
hind-foot ; ?, spiral shell.
Fio. 77. — Operoulnm of Splrialls enlarge(L
to surround the head, and by the functionally important
BILOBAIION Of THE MJD-FOOT.
Two vei-y distinct branche,s of the Cephalopoda are to
be recognized : the one, the Pteropoda, more archaic in
the condition of its bi-
lobed mid-foot, including
a number of minute, and
in all probability degen-
erate, oceanic forms of
simplified and obscure
organization ; the other,
the Siphonopoda, con-
taining the Pearly Nau-
tilus and the Cuttles,
which have for ages (as
their fossil remains show)
dominated among the in-
habitants of the sea, be-
ing more highly gifted
in special sense, more
varied in movement,
more powerful in pro-
portion to size, and more
heavily equipped with
destructive weapons of h'bcsorwing-iikefinso'ttiiemi(f-iootr
oilence than any other marine organisms.
Branch a.— PTEROPODA
Characters. — Cephalopoda in which the mid-region of
the foot is (as compared with the Siphonopoda) in its more
primitive condition, being
relatively largely developed
and drawn out into a pair
of wing-like muscular lobes
(identical with the two halves
of the siphon of the Siphon-
opoda) which are used as
paddles (see figs. 76-86). The
hind -region of the foot is
often aborted, but may carry
an operculum (figs. 76, 77).
The fore-region of the foot
(that embracing the head) is
also often rudimentary, but
may be drawn out into one
or more pairs of tentacles,
simulating cephalic tentacles,
and provided with suckers
(figs. 84, 85).
Though the visceral hump
is not twisted except in the
Limacinidas (fig. 76), there is
a very general tendency to
one-sided development of the
viscera, and of their external
apertures (as contrasted with
Siphonopoda). The ctenidia
are aborted, with the possible
exception of the processes (fig.
85, c) at the end of the body
of Pneumodermon. Ths vas-
cular system resembles that
of the Gastropoda. The ne-
phridium is a single tubular rio. •a.styUoia acicuia. Bang. ip.
body corresponding to the Jf.r.lJ.T",'? .?r.;f. , ?'.'': ?'_!5
right nephridium of the typi-
cal pair of the archi-MoUusc.
The anal aperture is usually "• ""■•; ■-'^ i'=™''-<ri'"'dite gonad,
placed a little to the left of the median line, mora rarely
to the right. In the Limacinidse it has an exceptional
position, owing to the torsion of the visceral mass, as in
Anisopleurous Gastropoda.
XVI. — 84
... "lop
lilce lobes of the mid-foot ; d, mediAD
fold of same ; e, copulatory organ ; %,
pointed extremity of the sheU; i, an-
tenor margin or tlie shell; n, stomach-
666
MOLLUSCA
[SIPHONOPODA.
Jaws and a lingual ribbon are present as in typical
Glossophora, tha dtntition of the ribbon and the number of
jaw-pieces presenting a certain range of variation. Sense-
C
Flo. 79. — Cavolinia trUhtitota, Forfik. from rno McditerraDean, magnified two
tUameters (fiom Owen), n, mouth ; h, pair of cephalic tentacles ; C, C, ptero.
podial lobes of the mid-foot ; d, median iveb connecting these ; «, e, proceasea
of the mantle-altirt reflected over the surface of the shell ; g, the ahell en-
closing tlio visceral hump; ft, the median spine of the shell.
Flo. ea — Shell of Cavotinia trUUntata, seen from the side. /, postero-doraal
Burfhce ; g, antero-Tcatral surface ; A, median dorsal spine ; t, mouth of the
>hell
organs are present in the form of cephalic eyes in very few
forms (Cavolinia, Clione, and in an undescribed form dis-
covered by Suhm during the "Challenger" Expedition); oto-
cysts are universally present. The osphradia are present
in typical form, although the ctenidia are aborted ; only
one osphradium (the
right of the tjrpical
pair) is present (fig.
87). The gonads aro
both male and female
in the same individual.
The genital aperture is
single. Copulatory or-
gans, often of consider-
able size, are present
(fij-'-SG,.).
The mantle-skirt is
present in one divi-
sion of the Pteropoda
(Thecosomata), and in
these an extensive sub-
pallial chamber is de-
veloped, the walls of
which in the absenco
of ctenidia have 9
branchial function. In
a second division (Gym- p,n. Sl.-Embryo of CavoUnia trtdinlata(trom
nosomata), which com- '^'/l""; """■ ^'''■'; "• ""I'.'; ^ "='';''?, P^r"""
. '' , . of the foot; pn, pteropouial lobe of the foot;
prises forms highly de- ft, heart ; i, intestine ; o(, otocyst ; q, shell ; r,
vr-lnnpH in rpirnrrl in nephridlum ;», ojsophagua ; ir, sac containing
>C10pea in regara to nutritive yollc; vii, mantle-skirt; me, sub-
the processes of the pallial chamber ; Kn, coutractile sinus.
fore-foot, the mantle-skirt is aborted. A shell is developed
on the surface of the vi.sreral hump and mantle-skirt of the
Thecosomata, whilst in the Gymnosomata, which have no
mantle-skirt, there is in the adult animal no shell. The
embryo passes through a trochosphere and a veliger stage
(fig. 81), provided with boat-like shell, except in some
Gymnosomata in which the Trochosphere with its single
velar ciliated band becomes metamorphosed into a larva
which has three additional ciliated bands but no velimi
(resembling the larva of the Scaphopod Dentalium) ; this
banded larva does not form a larval shell (fig. 84).
Tlie Pteropoda aro divided into two order.s.
Order 1. — Thecosomata.
Characters. — Ptcrojjoda provided with a laantla-skirt,
and with a delicate hyaline shell developed on the surface
of the visceral hump and mantl6«kirt ; visceral hump, and
consequently the shell,
spirally twisted in one
family, the Limacinidas;
shell often with con-
tracted mouth and di-
lated body, its walls
sometimes drawn out
into spine-like processes,
which are covered by
reflexions of the free
margin of the mantle
(Cavolinia, figs. 79, 80).
Family 1. — Cymb^Uiidm.
Genera : TicdcTnannia,
Chj. ; Halopsyche, The-
aunjhia (tim, 82, 83),
Cymbulia^ P. and L.
(fig. 77a).
Family 2. — Conulariidm
(fossil).
Genus : Coilularia, Mill.
Family 3. — TattaculUidm
(fossil). Fio. Sl. — TTuKvTyMa eandlchauM, 8onl.,
Genera : TentaculiUa, C^" Owenji Much enlarged ; the body-»10
Q-i-ui, . n .7,-*- removed, a, the month ; c, the pt^ropodtai
Schth. ; Comulilcs, ,„^ „, ^-^ ,^^. y- the centiillv- plow*
Schlth. ; ColcQpnon, hind-foot ; <J, I, «, three pairs of tentode-Uke
Sandb. processes placed at the sides of th* moatH.
and developed (in all probability) from the
fore-foot ;o, anus; y, genital pore ; t, retnict«c
genitalia.
Family 4. — fftjaleidm.
Genera: Triptera, Q. ^na musdea; oand c,':
G. ; Slyliola, Lcs, (fig. ' '
78) ; Balantium, Lch. ; Vagindla, Dand. ; Cleodor
L. ; Dlacriitf Gr. ; flcurofnta, Esch. ; Cavolinia, G
79, 80, 81).
Family 5. — Thccidm.
Genera : Tluca, Low ; PUrothixa, Salt
Family 6. — Liviacinidas.
Genera : Ikcylioviphahis, PortL ; Hd^mfnsMji, Fig. ;
Spinalis, E. S. (fig. 76); Limacina, Cuv.
Order 2.— Gynuiosoinata.
Characters. — Pteropoda devoid of mantle-
skirt and shell; tentacular processes of the
fore-foot well developed and provided with
suckers. f J
Family 1. — Pteroq/modoceidcS.
Genua : Pteroci/modoce, Ke£ f 'c- 83.— 3heH
Family 2.—Clionidm. ^„ '^oS'
Genera: Cliodita, Q. and G. ; Clionopsis, Trosth. ; tnslt; the
Olione, Pall. (fig. 86). lower flgnrt
Family S.—Pneumodermidm. tmZ\ul'^'
Genera : Trichocycliis, Each. ; Spcngohrmichia,
d'Orb. ; Piienmodermopsis, Kef. ; Pntitmoda-nion, Cuv. [^g. 85).
Branch h.—SIPHOA'OrODA.
Cephalopoda in which the two primarily divergent right
and left lobes of the mid-region of the foot have their free
borders recui-ved towards the middle line, where they are
either held in apposition (Tetrabranchiata), or fused with
one another to form a complete cylinder open at each end
(Dibranchiata). This fissured or completely closed tube is
the siphon (fig. 75, (C), mf) characteristic of the Siphono-
poda, and is used to guide the stream of water expelled
by the contractions of the walls of the branchial chamber.
The pallial skirt i.s accordingly well developed and muscular,
subserving by its contractions not only respiration but
locomotion. The visceral hump is never twisted, and ac-
cordingly the main development of the pallial skirt and
chamber is posterior, the excretory apertures, anus, and
gills having a posterior position, as in the archi-Mollusc
At the same time the visceral hump is usually much elon-
gated in a direction corresponding to an oblique lino be-
tween the vcEtical dorso-ventral and the horizontal ant-ero-
postcrior axes (see fig. 75, (0)).
Sn>HON0SPDA<]
MOLLUSCA
667
The for©-part of the foot which snrrotmds the month, as
in all Cephalopoda, is drawn out into four or five pairs of
lobes, eometimes shorty but osually elongated and even fili-
Fig. 84
Pio'. M.— terra of Patuttodermon (from
E-oral ciliated band of the trochosphe]
Fig.
Balfonr, after GegenbenrX
the mdimente of a pair of processes growing from the head. In Bttc fore-
moet ciliated ring has disappeared ; the cephalic region is greatly developed,
&nd, as comparedwlth the adult (fig. 85X is large and free ; the pair of hook-
bearing processes on each side of tie mouth .ire retractile, probably part of
the fore-foot At the base of the cephalic suont are seen the pair of arm-
like processes (fore-foot) provided with 6nck':rs, and behind these the broad
pteropodial lobes or wing-like fins of the raid-foot
Pio. 85. — PTieumodtrmon violaceum, d'Orb, ; magnified five diameters, a, the
sncber-bearing anna ; 6, the flns of the mid-foot (in the middle line, between
theee, la seen the sucker-like median portion of the foot, by nif-aus of which
the animal can ctawl as a Gastropod) ; c, tBe foor branchial processes. (After
Kefei^ln.)
form. These lobes either carry peculiar sheathed tentacles
(Nautilus), or, on the other hand, acetabulif orm suckers, which
may be associated with claw-like • hooks (Dibranchiata).
The hind-foot is probably represented by the valve which
depends from the inner
w^ of the siphon in
many cases. ^—■''~~~*^4Si I-
A sheU (figs. 89, 100) .'^-— s^-« .
ia very generally present,
afiFording protection to
the visceral mass and
attachment for muscles.
It may be external or en-
closed in dorsal UpgrOW- Fio. 86,— Oion* !>or.-a!ij, L. ; magnified two
lag folds of the mantle, """ "~
which (except in Spirula)
■ L ■ 1 .J uiciuuo uiiiiui-o 8u[;Kt;r-UKe processes, a
Close up at an early penOa snrrounded by a hood-like upgrowth.
of development, so as to '","' '■„?''* more elongated tentacles (the
i/» uoTo.uyujouv, =>.. ,. retractile cye-tentaolcs are not seen, being
form a shut sac m which < phiced dorsaUy); c, the pteropodial llns;
»).o cTipIH.. Ofx-rpi sH T>iB ■*■ *' median portion of the foot ; o. the
tne snell 13 secret ea. ine anus ; y, the vagina ; j, the penl^ (From
ctenidia are well deve- Owen, a-icr Escimcht)
loped as paired gill-plumes, serving as the efSoient bran-
dual organs (figs. 101, 103,
and fig. 2, B).
The vasciilar system ia
Tery highly developed ; the
heart consists of a pair of
auricles and a ventricle (figs.
104, 105). Branchial hearts
are formed on the advehent
vessels of the branchiaj. It
is not known to what extent
the minute subdivision of
the arteries extends, or
whether there is a true
capillary system.
The pericardium is ex- 6el.,»fer Sonleyet). Cei!,'nghtcerc-
■ , "^ . , bnil gangbon; Pl.R, right pleural
tended so as to lOrm a very ganglion ; Pt, right pedal ganglion ;
large sac passing among [^';^^^r,^'^^i^-4^''^'^'^%t
the viscera dorsal wards and tro-pedal connective ; cpU right cere-
.. ^„„x«.:„* „ *i.„ bro-pleural connective: Osp., osphra-
eometimea containing the dinm connected by a nerve V/itfi the
ovary or testis — the viscero* ^e^^ visceral gaogUoa
pericardial sac — which opens to the exterior either directly
or through the nephridia. It has no connexion with the
vascular system. The nephridia are always jpaired sacs,
the walls of which invest the branchial advehent vessel*
(figs. 104, 108). They open each by a pore into the viscero-
FiQ. S8.— Male (nppcr) and female nower) flpecJmens of Nautiha jxmptilus ss
aeen in the expanded condition, tbe obsen'er looking down on to the bDccal
cone e ; one-third the natural size linear. The drawings have been made
from actual specimens by A. G. Bourne, B.Sc, and serve to ahow the
natural dispo:'itlon of the t^ntaculiferoua lobes and tentacles of the circiun-
oral portion of tlie foot (n the living state, as well as the great differences
between the two sexes, a, the shell ; 6, the outer ring-like expansion (annular
lobe) of the circnm-oral muacular mass of the fore-foot, canTing nintteeB
tentacles on each side — posteriorly this ia enlarged to form the "hood"
(marked v in flg. 89 and m. in figs. 90 and 01), giving off the pair of tentaclef
marked g in the present figure ; c, the right and left inner lobes of the fore*
foot, each carrying twelve tentacles In ihe female, in the male enbdivided
intoji, the "spadix" or hectocotylna on the left side, and g, the " anti-spadix,"
a group of four tentacles on the right side,— it is thus seen that the subdivided
right and left Inner lobes of the male correspond to the undivided right and
left inner lobes of the female ; d, the inner inferior lobe of the fore-fc'jt, a
biiatei-al structure in the female carrying two groups, each of fourteen tenta-
cles, separated from one another by a lamellated oi^a ts supposed to be
olfactory in function— in the mole the inner inferior lobe of the fore-fcct ij
very much reduced, and has the form of a paired group of lamellse (d in the
npper figure); e, the buccal cone, rising from the centre of the three inner looee,
ana fringing tbe protruded calcareous beaks or jaws with a series of minute
papillie ; f, the tentacles of the outer clrcum-oral l&be or ^Ttnilar lobe of the
fore-foot projecting from their sheaths ; g, the two most posterior tentacles
of this series belonging to that part of the annular lobe whidi forms the
hood (tji, in figs. 90 and 91); i, superior ophthalmic tentacle; it, inferior
ophthalmic tentacle ; I, eye ; m^ paired laminated organ on feach side of the
base of. the inner inferior lobe (d) of the female, probably olfactory in fiiDO-
tion ; n, olfactory lamellEB npon the inner inferior lobe (in the female) ; o,
the siphon (mid-foot) ; p, the spadix (in the male), the hectocot>-lized portlan
of tho left inner lobe of the fore-foot representing four modihed tentacles,
eight being left nnmodifled ; q, the anti-spadix (in the male), being four of
the twelve tentacles of the right inner lobe of the fore-foot isolated from
tho remaining eight, and representing on the right side the differentiated
spadix of the left side. The four tentacles of the anti-spadix are set, thrM
on one base and one on a separate base.
There are thus in the female, where they are most numerous, nlnet>--four
tentacles, thirty-eight on the outer annular lobe, four ophthaliiuc (a pair to
each eye)i twelve on each of the right and left inner lob^ and twenty-eight
on the inner Inferior lobe.
pericardial sac except in Nautilus. The anal aperture is
median and raised on a papilla. Jaws (fig. 88, e) and a lin-
gual ribbon (fig. 107) are well developed. The jaws have
the form of a pair of powerful beaks, either homy or calcified
(Nautilus), ^d are capable of inflicting severe wounds.
668
MOLLUSCS
[SIPHONOPODA.
Sense-organs^are highly "developed ; the eye exhibits a
very special elaboration of structure in the Dibranchiata,
and a remarlcable archaic form in the Nautilus. Otocysts
are present in all. The typical osphradium is not present,
! Of the female Pearly Nautilus, contraeted ty spirit and lying in its shell,
'""'' '■ "■■* — ay (frora_ Qegenbaur, after Owen), a, visceral hnmp; 6,por-
term hectocotylization is applied to this modification (see
figs. 88, 95, 96). Elaborate spermatophores or spemi-ropes
are -formed by all Siphonopoda, and very usually the female
possesses special capsule-forming and nidamental glands for
providing envelopes to the eggs (fig. 101, ff.n.).
The egg of aU Siphonopoda is large, and the
development is much modified by the presence
of an excessive amount of food-material diflFused
in the protoplasm of the egg-cell. Trochosphere
and veliger stages of develooment are conse-
quently not recognizable.
The Siphonopoda are divisible into two
orders, the names of which (due to Owen) de-
scribe the number of gill-plumes present ; but
in fact there are several characters of as great
importance as those derived from the gills by
which the members of these two orders are
separated from one another.
Order 1. — TetrabraacUiata ( = Schizosiphona,
Teniae uiifera).
Characters. — Siphonopodous CepnaiopodS
in which the inrolled lateral margins of tba
mid-foot are not fused, but form a ciphon by
apposition (fig. 101). The circum-oral lobes
of the fore-foot carry numerous sheathed ten-
tacles (not suckers) (fig. 88). There are two
pairs of ctenidial gills (hence Tetrabraiichiata),
and two pairs of nephridia, consequently four
nephridial apertures (fig. 101). The viscero-
pericardial chamber opens by two independent
Hro. 89.— literal \
the right half of which is cut l _
aonofthefreeedgeofthemantlo-sWrtreflectedon to the shell,— tlie edge of the mantic-akiri; nnp'tlirp? to ttip pxtprior and not into thp
canbetraceddow-nwardaandforpaitisaroundthebaseottheiiid.footorsiphcml; ^i.suMr.'^P , ., , ''° """^ exi^nor ana noi into tne
flcial origin of the retractor muscle of the midfoot (siphon), more or less firmly attached to the nephfldial sacs. There are two OVlductS
shell, of which a small piece (a) is seen between the letters M • s ^farther back^ rtolnts to the / ■ t ^ i i r, \ • xt. ^ i j i
siphuncuiarpedicie,whi?hisbrikenofrsbortl?dnotcon«ruyWifthepeS^^^^ ("gilt ^^d left) m the female and two sperm-
tho whole length of the siphmicle of the shell, also marked » and «■ ; o points to the right eye ; ductS in the male, the left duct in both
< is placed near the extremities of the contracted tentacles of the outer or annuhir lobe of the , . , • 1
Tore-foot,— the Jointed tentacles are seen protruding a little from their long cylindrical sheaths ; r, SexeS being rudimentary.
foo\t"fi l^r^'J^t tlT.,^irZ^i.^^^litZ^L:^l Sr;?siJ,o^c"n t!^SX. ^ l"g« «^t«'?al ^^^^^ ^^'"^^^ eoUed or straight
isce of the nidamental gland (see Og. 101, g.ii.). is present, and IS not enclosed by reflexions of
except in Nautilus, but other- organs are present m tne the mantle-skirt, except such narrow-mouthed shells as
that of Gomphoceras, which wore probably enclosed by the
Bonme). wlj the dorsal "hood " formed by the enlargement of the outer
annular lobe of the fore-foot, and corresponding to the sheaths of two tenta-
cles (ff, 17 in flc. 88) ; n., tentacular sheaths of lateral portion of the annular
lobe ; «., the led eye ; ft., the nuchal plat£, continuous at its right and left
posterior angles with the root of the mid-foot, and corresponding to the
nuchal cartilage of Sepia; c, visceral hump; d., the free ma'-rin of the
mantle-skirt, the middle letter d. points to that portion of the mantle-skirt
which is reflected over a part of tlie shell as seen in fig. 89, 6 ; the cup-like
fossa to which 6. and d. point in the present figure is occupied by the coil of
the shell ; i;.a. points to the lat'^ral continuation of the nuchal plate b. to
Join the root of the mid-foot or siphon.
cephalic region, to which an olfactory function is ascribed
both in Nautilus and in the other Siphonopoda.
The gonads are alvv-ays separated in male and female
individuals. The genital aperture and duct is sometimes
single, when it is the left ; sometimes the typical pair is
developed right and left of the anus. The males of nearly
all Siphonojioda harve been shown to bo characterized by a
peculiar modification of the arm-like processes or lobes of
the fore-foot, connected with the copulative function. The
Flo. 91.— Lateral view of the same specimen as that drawn in fig. Oa Lett«l»
as in that figure with the following additions— f points to the concave m: i-gln
of the mantle-skirt leading into the sub-palllal chamber ; g, the mid-io a or
siphon ; k, the superficial origin of itji retractor muscles closely applie l to
Uie shell and serving to hold the animal in its place ; I, the siphnncular pedicle
of the visceral hump broken off short ; v, v, the superior and inferior ophthal-
mic tentacles.
mantle as in the Dibranch Spirula. The snell consists of
a series of chambers, the last formed of which is occupied
by the body of the anin%^l, the hinder ones (successively
deserted) containing gas (fig. 89).
The pair of cephalic eyes are hollow chambers (fig. 118,
A) opening to the exterior by minute orifices (pinhole
camera), and devoid of refractive structures. A pair of
osphradiaare present at the base of the gills (fig. 101, o//).
Salivary glands are wanting. An ink-sac is not present.
Branchial hearts are not developed on the branchial advo-
hent vessels.
8IPH0:<0P0DA.]
MOLLUSCA
66S
Flmily 1. — yaiUilufsB.
Genera: [Orl/uxcras], Breyn.; [Cijiiceerus], Goldfuss; [Omnji/io-
aim], Uiisster ; (Phratpjioaras^ Brod. ; [Gijroceraa], ilojer
[Aseoce)as\ Barraude ; [Oncocer(is\ Hall; {Liluites\ Breyn.
\Troch<xeras\ Barraude; KautUus, L. (figs. 88, 89, 90, &«.)
[Clymenia], Miinst. ; {Xothoeeraa], Bahaude.
Family 2. — Ai'imoniivias.
Genera : [SnctriUa], Sanderg. ; [OoniaiUca], d? Haan ; [Rhaido-
ceras], Hauer ; [Clydouites], Hauer ; [CocAloccras], Haaer
[Baculina], d'Orb. ; [CeraliUs], de Haan ; [Baculita], Lam.
[Toxoaras],d'Orh.; [Crioceras], heyeilli ; [Pli/chocera3],i'Oib.
[ffamiUs], Parkinson ; [Anajloceras], d'Orb. ; [Seaphila],
Parkinson ; [Ammonita], Brevn. ; [Turrilitfs], Lam. ; [Bclia-
cfTOj], d'Orb. ; [Ilttcroceras], d'Orb.
If.B. — The names in brackets ale those of extinct genera.
Order 2. — Sibranchiata ( = Holosiphona, Acetabulifera).
CharacUrs. — Siplionopodou3 Cephalopoda in which the
inflected lateral margins of the mid-foot are fused so as to
form a complete tubular siphon (fig. 96, t). The circum-
oral lobes of thf fore-foot carry suckers disposed upon them
in rows (as in the Pteropod Pneumodermon), not tentacles
(see figs. 92, 95, 96). There is a single pair of typical
xrtenidia (fig. 103) acting as gilb (hence Dibranchiata), and
1 when dead, tne lev
Fio. Qi.—Stpia oJJlclihUlf, «,, half the natural sit*, «.. o^ „ .. ii^.. u=bm, »uo luu^
preheDiUe arms being witbdrart-n from the pouches at the aide of the head,
finally in use. ti, Deck;
;ed during life when not i
\ lateral fin of the mautlc-sac ; c, the eight shorter a
the two long prehensile arms ; e, the eyes.
1 of the fore-foot ; d,
a single pair of nephridia opening by apertures right and
left of the median anus (fig. 103, r), and by similar internal
pores into the pericardial chamber, which consequently does
not open directly to the surface as in Nautilus. The ovi-
ducts are sometimes paired right and left (Octopoda),
sometimes that of one side only is developed (Decapoda,
except Ommastrephes). The sperm-duct is always single
except, according to Keferstein, in Eledone moschata.
A plate-like shell is developed in a closed sac formed by
the mantle (figs. 98, 99), except in the Octopoda, which have
none, and in Spirula (fig. 100, D) and the extinct Belemni-
tidsB, which have a smaill chambered shell resembling that
of Nautilus with or without the ^diiicu of plate-lik^ and
cylindrical accessory developments (fig. 100, C).
The pair of cephalic eyes are highJy-develoi,ed vesicles
with a refractive lens (fig. 120), cornea, and lid-fclds, — thf
vesicle being in the embryo an open sac Uke that of Nautilut.
(fig. 119). Osphradia are not preset t, but cephalic olfac
tory organs are recognized. One or two pairs of large
salivary glands with long ducts are present. An ink-sac
formed as a diverticulum of the rectum and opening neai
the anus is present in all Dibranchiata (fig. 103, t), and ha.<
been detected even in the fossil Belemmtidse. Branchia
hearts are developed on the two branchial advehent blood
vessels (fig. 104, tx, vi).
The Dibranchiata are divisible into two sulMirders, accord
ing to the number and charact;r of the arm-like sucker
beating processes of the fore-foot.
Pio. 03.— DecApodons Slphonopods ; one-fonrtli the ttatatal BiM linear. A
LlitiroteiiOiii Vci-anyi, d'Orb. (Crom the Mediterranean), B. Tttytaiiotniki^
rhombus, Troschel (Crom Measina). C. LollgoptU cyaunj. Fix. and d''Orb
(from Oio AOanUc Ocean).
Sub-order 1. — I>ecapoda.
Character}. — Dibranchiata with the fore-foot drawn out int'
eight shorter and two longer arms (prehensile arms), the latter bein^
placed right and left between the third and fourth shorter arms
The suckers are stalked, and strengthened by a horny ring. Th-
eyes are large and have a hoi-izontal in place of a sphincter-Tike lid
The body is elongated and provided with lateral fins (lamellifom-
expansions of the mantle). The mouth has a buccal membrane
The mantle-margin is locked to the base of the siphon by a specially
developed cartilaginous apparatus. Kumerous water-pores are pre
sent in the head and anterior region of the body, leading into re
cesses of the integument of unknown significance. The oviduct i-
single ; large nidamental glands are present The viscero-pericar
dial space is large, and lodges the ovary (Sepia). There is alway-
a shell present which is enclosed by the upgrowth of the m&ntle.
so as to oecome "intemah"
Section a. — Decapoda Calciyhora.
Chanuicr. — Internal shell calcareous.
Family 1. — SpiruUdm.
Genus : Spirula, Lam. (fig. 100, D).
Family 2. — BcUjnnitidm.
Genera : [Spirulirotlra], d'Orb. (fig. 100, C) ; [Belopterj], DtaL ,
[BcUmno^sl Edw. ; [ConoUvtltu], d'Orb. (fig. 100, A) ; [Acan
tlwtaUhis], &. Wag. ; [Bclemniica]^ Lister, 1678; [BeletanOellal
d'Orb.; [XiphoUvthis), Huxley.
Family 3. — Sepiadec.
Genera: Sepia, L. (figs. 92, 98, tt); [Bcloxpia], Yolt»; Coew-
Uuthis, Owea
670
M O L L U S
Section I. — Deeapoda Cliondrophora.
CharaeUr. — Internal shell homy.
Sub-section o. —Myopndx (d'Orb. ).
Eye with clawed cornea, so that the surronndiiig water does no
touch the lens ; mostly frequenters of the coast
Family 1. — Loligidm.
Genera: Loligo, Schneid. (figs. 99, &c.); LoKolus, oceenstrnp ;
SepioteiUhis, Blv. ; [TeuUwpsisl Desl. ; [LeptoUuthisl Meyer;
[Belemnosepia], Ag. ; [Beloteuthis], Miinst
Family 2. — Scpiolidm.
Genera : Sepiola, Schneid. ; Ro3sia, Owen.
Sub-section p.—Oigopsidm (d'Orb.).
Eye with open cornea, so that the surrounding water bathes the
anterior surface of the lens ; mostly pelagic aainmls.
Family Z.—Cranchiadm.
Gtnus : Oranchia, Leach (fig. 94, C).
Family 4. — Loligopaids.
Genus : Loligopsis, Lam. (fig. 98, C).
Family 5. — CheiroteutkidaB.
Genera : Clmiroteuthis, d'Orb. (fig. 93, A) ; Bistioteuthis, d'Orb.
Family 6. — ThyaanotciUhidss.
Genus : Thyscmoteuthis, Troschel (fig. 93, B).
Family 7. — OnycTioieuthidBS.
■nera : Gonatiis, Gray ; Onychotmthis, Lichtenst (fig. 97) ; Ony-
chia, Lesueur ; Bnoploteuthis, d'Orb. , Veranya, Kjohn ; [Plesio-
tailhis], A. Wag. ; [Celes7u>\ Miinst : riotidiais, Steenstrup ;
Ommastrcphes, d'Orb.
Sub-order 2. — OdOfioda.
CliaTocters. — Dibranchiata with the fore-foot drawn out into eight
arms only; suckers sesaile, devoid of homy ring; eyes small, the
Fio. 04.— Octopodoua Siphonopods ; one.fonrtli tlie natural size linfar. A.
Pinnixtojms cordtMmis, Quuy and Gala (from New Zealand). B. Tremoc-
hprn violacm, Ver. (from the Medltermnoan). C. OranAia scabra Owen
(from the Atlantic Ocean j one of the DecaiKxla). D. ClrrhotntthU MMUH,
E5ch. (from the Greenland coaat).
outer skin can be closed over them by a sphincter-like movement
The body is short and rounded ; the mantle has no cartilaginous
locking apparatus, and is always fused to the head dorsally by a
broaJ nuchal band. No buccal membrane surrounds the mouth.
The siphon is devoid of valves. The oviducts are paired ; there are
no nidamental glanda The viscero-pcrieardial apace is reduced to
two narrow canals, passing from the iiophridia to the capsule of tl'e
genital gland. There ia no shcll.on or in the visceral Iiump.
Family l. — Cirrhottuthidm.
Genus: CirrhoUulhiii, Each. [Sciadtphorus, Roinh.) (fig. 94, D>
Family 2. — Ociopodida.
Genera ; Pinnoctopiu, d'Orb. (fig. 94, A) ; Octopus, Lam. (fig. 95) ;
ScaeuTgxis, Trosch. ; Elaione, Leach ; Bolitmna, Steenstrup.
J .A. • [c3rilA10r01)A.
Family Z. --~'\Jfmczid^.
Genon : T , .nwclopua, Delle Chiaje (Philonexii, d'Orb.) (fig. 94,
B) ; .'-r 'ra, Stoi.?JEtrup (Odopus catenulatta, Fer., is the
femrilf . -. u Octopus carciui, Ver, ia the male of the one species
of tl " IU3 according to Steenstrup (fig. 96}) ; Arg(maiUa, L
(the : '. i' of this genus ia formed only in the female by the
(rpanJi: i enda of the two largo " arms " of the fore-foot).
PiQ. 05.— A. r-rilc specSmon of Octopus ffrcmlandtc^tt, with the thW arm of th»
right side hcctocotylUed. B. The extremity of the hectocotjlUed arm
magnlHed.
Fvrther Remarks on the Cephalopoda. — In order to give
a more precise conception of the organization of the Cephalo-
poda, in a concrete form we select the Pearly Nautilus for
further description, and in pass-
ing its structure in review we
shall take the opportunity of
comparing here and there the
peculiarities presented by that
animal with those obtaining in
allied forms. In the last edition
of this work the Pearly Nautilus
was made the subject of a dr-
tailed exposition by Professor
Owen, and it has seamed accord-
ingly appropriate that it should
be somewhat fully treated on
the present occasion also. The
figures which illustrate the pre-
sent description are (excepting
fig. 89) original, and prepared
from dissections (made under the
direction of the writer) of a male
and female Katililvs pompilivs,
lately purchased for the Musouni
of University College, Loudon.
Visceral ITKmp end Shell. —
The visceral hump of Nautilus
(if we exclude from considera- _
tion the fine sijihuncnlar pedicle fio. S6.— Male of farojim cv>rM-
which it trails, as it v,-ere, behind v\'?:,\'^^n™?hfh"«t"otyU?3
it) is very little, if at all, affected arm. n, e. P, n, the Urst, lecond,
, ' ,, ■. 1 i t lu 1, 11 third, and fourth aims or pro-
by the coiled form of the shell cesses of thj forefoot ; A, the
which it carries, since the animal ^J^^ST:"'. ufe "^5^?'^ oT^i
always slips forward in the shell hcctocotv'uied arm ; v, the fiu-
as it gi-ows, and inhabits a cham- ^^^ t'eiopmen't S""ompi«5 •
ber which is practically cylindri- i, the siphon. (From Qceeni«ur.)
cal (fig. 89). Were the deserted chambers thrown off instead
of being accumulated behind the inhabited chaml:)er as a
coiled series of air-chambers, we should have a more correct
indication io the shell of the extent and form of the animal'*
CXPHALOFODJu]
MOLLCJSCA.
671
body. Amongst Qastropod-i it is not very unusual to find
tho animal slipping forward in its shell as growth advances
and leaving an unoccupied chamber in the apex of the shell.
ThiSTnay indeed become shut off from the occupied cavity
by a transverse septum, and a scries of such septa may be
formed (fig. 42), but in no Gastropod ore thcie apical
chambers known to contain a
gas during the life of the
animal in whose shell they
occur. A further peculiarity fi
of the Nautilus shell and of
that of the allied extinct Am-
monites, Scaphites, Orthoceras,
(Sx., and of the living Spirula,
is that the series of deserted
air-chambers are traversed by
a cord -like pedicle extending
from the centro-dorsal area of
the visceral hump to the small-
est and first-formed chamber of
the series. No structure com-
parable to this siphunctilar
pedicle is known in any other
Mollusca. Its closest repre-
sentative is found in the so-
called "contractile cord" of
the remarkable form Rhabdo-
pleui-a, referred according to
present knowledge to the Poly-
zoa. There appears to be no
doubt that the deserted cham-
bers of the Nautilus shell con-
tain in the healthy living
animal a gas which serves to
lessen the specific gravity of
the whole organism. The gas
is said to be of the same com-
position as the atmosphere,
with a larger proportion of
nitrogen. With regard to its
origin we have only conjec-
tures. Each septum shutting jj^
off an air-containing chamber
is formed during a period of
quiescence, probably after the
reproductive act, when the vis- j
ceral mass of the Nautilus may
be slightly shrank, and gas is
secreted from the dorsal inte- '■
gument so an to fill up the
space previously occupied by
»i.„ „„; 1 * *„• „i Fw. 87 — Head and cIrcaTnK>l-al pro-
the animaL A certam stage cc»sea of the fore-foot of Onycho-
is reached in the growth of teuthls (from Owen^ a. neck ; b,
^^ _. , 1 _ _ _ I, eye : c. tlic eight short RHUS : rf, long
" prehcrwile arms, the clavato extre-
the animal when no new cham-
prOCeSS of the loosening of the of hooka beyond at/. The tempo-
• 1 ■ -i 1. 1 J c rary conjunction of tho amis by
aruinal m its chamber and Ot meana of the suckers enables them
its slipping forward when a » act i" i:<""Wn;ti™
new septum is formed, as well as the mode in ■ivhich the
air-chambers may be used as a hydrostatic apparatus, and
tlie relation to this use, if any, cf the siphuncular pedicle,
if involved in obscurity, and is tho subjf.ct of much in-
genious speculation. In connexion with the secretion of
gas by the animal, besides the parallel cases ranging from
the Proteroon Arcella to the Physoclistic Fishes, from
the Hydroid Siphonophora to the insect-larva Corethra,
wo have the identical phenomenon observed in the closely-
allied Sepia when recently hatched. Here, in the pores
of the internal rudimentary shell, gas is observable, which
has necessarily been liberated by the tissues which secrete
the shell, and not derived from any external source
(Huxley).
The coiled shell of Nautilus, and by analogy that of the
Ammonites, is peculiar in its relation to the body of tho
animal, inasmuch as ftie curvature of the coil proceeding
Fig. 98. Fig. 90.
Fio. 08 The calcareons Internal shell cf Scpin nffiiinalh. the so.called cuftlc-
bone. Oj lateral expansion ; t, anterior canceUntod region ; c, Lauiiuated
region, the laroinpe enclosing air.
Pio. 99.— The homy internal shell or gladlus or pen of Loligo.
from the centro-dorsal area is towards the head or forward,
instead of away from the head and backwards as in other
discoid coiled shells such as Planorbis ; the coil is in fact
absolutely reversed in the two cases. Amongst the extinct
allies of the Nauti-
lus (Tetrabranch-
iata) we find shells
of a variety of
shapes, open coils
such as Scaphites,
leading on to per-
fectly cylindrical
shells with chamber
succeeding cham-
ber in a straight
line (Orthoceras),
whence again wo
may pass to the
cork-screw spiree
formed by the shell
of Tiirrilftpq Fio- »00 — Internal shells of Cephalopoda Stpnono-
™ ., , r^ P«la- •^- Shell of Cotulmlhh diiplnia«a. d'Ol-U
Whilst the Tetra- (from the Kcocomian of France). B- ShcU of
branchiata, so far as
we can recognize
their remains, are
characterized by
these large chambered shells, which, as in Nautilus, were
with the exception of some narrow-mouthed forms such
as Gomphoceras but very partially covered by reflexions
of the mantle-skirt (fig. 89, b), the Dibranoliiata present
an interesting series of gradations, in which we trace —
(a) the diminution in relative size of the chambered
shell ; (i) its complete investiture by reflected folds of
the mantle (Spirula, fig. 100, D) ; (c) the concrescence
of Fran
■Jlediterranean). C. Shell
of Spinilinsira BflhnlU, d'Orb. (ti-om the Mio-
cene of Turin). The specunen is cot so as to show
in section the chambeicd sliell and the laminated
" guard " deposited upon its surface- D. Shell of
Spirilla Itct-is, Graj' (Kew Zealand).
672
MOLLUSCA
[CEPHALOI-ODA.
of the folds of the mantle to form a definitely -closed
shell-sac ; (</) the secretion by these mantle-folds or walls
of the shell -sac of additional laminae of calcareous shell-
aubstance, which invest the original shell and completely
alter its appearance (Spirulirostra, fig. 100, C; Belemnites);
(e) the gi-adual dwindling and total disappearance of the
original chambered shell, and survival alone of the calcare-
ous laminae deposited by the inner walls of the sac (Sepia,
fig. 100, B) ; (/) the disappearance of all calcareoas sub-
stance from the pen or plate which now represents the
contents of the shell-sac, and its persistence as a horny
body simply (Loligo, fig. 99); (g) the total disappearance
of the shell-sac itself, and consequently of its pen or plate,
nevertheless the rudiments of the shell-sac appearing in
the embryo and then evanescing (Octopus). The early
appearance of the sac of the mantle in which the shell is
enclosed, in Dibranchiata, has led to an erroneous identifi-
cation of this sac with the prmiitive shell-sac of the archi-
MoUusc (fig. 1), of Chiton (fig. 10, A), of Arion (fig. 69,
D, a), and of the normally-developing Molluscan embryo
(figs. 68 and 72***, sh). The first appearance of the shell-
sac of Dibranchiata is seen in figs. 121 and 122, its forma-
tion as an open upgrowth of the centro-dorsal area of the
embryo having been demonstrated by Lankester (34) in
1873, who subsequently showed (35) that the same sheU-sac
appears and disappears without closing up in Argonauta
and Octopus, and pointed out the distinctness of this sac
and the primitive shell-gland. The shell of the female
Argonauta is not formed by the visceral hump, but by the
enlarged arms of the foot, which are in life always closely
applied to it.
The shell of such Pteropoda as have shells (the Theceso-
mata) is excessively light, and fits close to the animal, -no
air-chambers being formed. ' It is important to note that
in this division of the Cephalopoda there is the same tend-
ency, which is carried so far in the Dibranchiate Siphono-
pods, for the mantle-skirt to be reflected over and closely
applied to the shell (e.r;., Cavolinia, figs. 79 and 80). But
in Pteropoda there is no complete formation of a closed
sac by the reflected mantle, no thickening of the enclosed
shell, no dwindling of the original shell and substitution
for it of a laminated plate. The variety of form of
the glassiike shells of Pteropoda is a peculiarity of that
group.
Head, Foot~ Mantle-skirt, and-Sub^ailial Chamber. — In
the Pearly Nautilus the ovoid visceral hump is completely
encircled by the free flap of iotegument known as mantle-
skirt (fig. 91, «^, e). In the antero-dorsal region this flap
is enlarged so as to be reflected a little over the coil of the
shell which rests on it. In the postero-ventral region the
flap is deepest, forming an extensive sub-paUial chamber,
at the entrance of which e is placed in fig. 91. A view of
the interior of the sub-palliad chamber, as seen when the
mantle-skirt is retroverted and the observer faces in the
direction indicated by the reference line passing from e in
fig. 91, is given in fig. 101. With this should be com-
pared the similar view of the snb-pallial chamber of the
Dibranchiate Sepia (fig. 103). It shoidd be noted as a
diS'erence between Nautilus and the Dibranchiates that in
the former the nidamental gland (in the female) lies on
that surface of the pallial chamber formed by the dependent
mantle-flap (figs. 101, ff.n. ; 89, 'n> whil.st in the latter it lies
on the surface formed by the body-wall ; in fact in the
foimer the base of the fold forming the mantle-skirt com-
prises in its area a part of what is unreflected visceral
hiirap in the latter.
The apertures of the two pair.s of ncpbridia, of the vis-
cero-pericardial sac,' of the genital dnct.s, and of the anus
;vre sho^vn in position on the body-wall of the jiaUial cham-
ber of Nautilus in fig.-*. 101, 102, There are nine apertures
m all, one median (the anus), and four paired. Besides
these apertures we notice ttm pairs of gill-plumes which
are undoubtedly typical ctenidia, and a short papilla (tha
o ?■"'
Fio. lOl.—View of the postero-yentral surface of a female Pearly NantilnB, tha
mantle-Bkirt (c) being completely reflcct-ed so as to show the innejr wall of
the sub-palllal chamber (drawn from nature by A. G. Bourne^ a, muscu-
lar band passing from the mid-foot to the integument ; b, the ■valve on tho
surface of the funnel-like mid-foot, partially concealed by the inrolled lateraJ
margin of the latter ; c, the maiitle-skirt retroverted ; an, the median anuj;
X, post-anaj papilla of unknown significance ; g.n., nidamental gland ; r.ov.,
aperture of ttie right oviduct ; l.ov., aperture of the rudimentary left oviduct
(pyriform sac of Owen); neph.a.^ aperture of tie left anterior" nephrldlum;
ncph.p, aperture of the left posterior nephridiura ; cificjier., left aperture of
the viacero-peri cardial sac ; olf, the left osphradium placed near tlie base of
the anterior gill-plume. The foiu' gill-plumes (ctenidia) are net lettered.
osphradium) between each anterior and posterior gill-plumf*
(see figs. 101, 102, and explanation). As compared with
this in a Dibranchiate, we find (fig. 103) only four aper-
Fio. 102.— Viflw of tlie postero-ventral surface of a male Pearly Nautilus, tiis
miiiitlf>-skiit;(o) being completely reflected so as to show the inner wnll of
the aubpallial chamber, and the four ctenidia and the foot cut short (drawD
from iiJiture by A. O. Bourne), pe., penia, being the enlai^d termination
of th« light spcrmutie duct; I.sit., aperture of the mdlmentar>' loft apenuatic
duct (pyriform sac of Oweny. Other letters as in flg, 101.
lures, viz., the median anus with adjacent orifice of the
ink-sac, the single pair of uephridial apertures, and one
asymmetrical genital aperture (on the left side), except in
female Octopoda and a few others where the genital
ducts and their apertures are paired. No visccro-peri-
cardial pores are jiresent on the surface of the pallial
chamber, since in the Dibranchiata the viscero-peri cardial
OKFHAIOFODA.]
MOLLUSCA
673
sac opens by a pore iiAiO each nepluidiam instead of
directly to the surface. A single pair of ctenidia (giU-
plnmes) is present instead of the two pairs in NaatUus.
The existence of two pairs of ctenidia and of two pairs
of nephridia in Nautilus, placed one behind the other, is
highly remarkable. The interest of this arrangement is in
relation to the general morphology of the Mollusca, for
it is impossible to view this repetition of organs in a linear
series as anything else than an instance of metameiic seg-
mentation, comparable to the segmentation of the ringed
worms and Arthropods. The only other example which
we have of this metamerism in the Mollusca is presented
by the Chitoas. There we find not two pairs of ctenidia
merely, but skteen poirs (in some species more) accom-
Tia. Ito.— View of thB postero-Veutral ^orCiee of a mala Septa, obtained oy
cutting longitndiLally the firm mantle-skirt and drawing the divided halves
apart Tbi^ lignre i^ strictly comparabk with Sg. 101, C, the head ; J, the
mid-foot or siphon, which has been cut open so as to display the valve » ; S,
the glandular tissue of the left nephridium or renal-sac, which has been cut
open (see fig. lOS) ; P, P, the lateral fins of the mantle-skirt ; Br, the single
pair of bianchise (ctenidja) ; a, the anus, — immediately below it is the open-
mg of the ink-hag ; c, cartilaginous socket in the siphon to receive c*, the
cartilaginous knob of the mantle-skirt, — the two constituting the "pallial
binge appaimtUB " characteristic of Decapods, not found in Octopoda ; g, the
azygos genital papilla and aperture ; '-., valve of the siphon (possiDly the rudi-
mentary hind-foot); m, musculai- bar.d connected with the fore-foot and
mid-foot (siphon) and identical with the muscular mass it in Sg. 61 ; r, renal
papillae, carrying the apertures of the nephridia; p.t>r, branchial efferent
blood-vessel ; cor', bulbous enlargements of the bi'snchial blood-vessels (see
Bgs. 1(M, 108) ; (, ink-bag. (Prom Gegenbaur.)
panied by a similar metamerism of the dorsal integument,
which carries eight shells. In Chiton the nephridia are
not affected by the metamerism as they are in Nautilus.
It is impossible on the present occasion to discuss in the
way which their importance demands the significance of
these two instances among Mollusca of incomplete or partial
metamerism ; but it would be wrong to pass them by with-
out insisting upon the great importance which the occur-
rence of these isolated instances of metameric segmentation
in'a group of otherwise unsegmented organisms possesses,
and the light which they may be made to throw upon the
nature of metameric segmentation in general.
The foot and head of Nautilus are in the adult inex-
tricably grown together, the eye being the only part belong-
ing primarily to the head which projects from the all-
embracing foot. The fore-foot or front portion of the foot
in Nautilus has the form of a number of lobes carrying
tentacles suid completely snrrounding the mouth (figs. 88,
89, 91). The mid-foot is a broad median muscular pioc^ss
which exhibits in the most interesting manner a curling in
of its margins so as to form an incomplete siphon (fig.
101), a condition which is completed and ren(lered per-
manent in the tubular funnel, which is the form presented
by the corresponding part of Dibranchiata (fig. 96). The
hind-foot possibly is represented by the valvtilar fold on the
surface of the siphon-like mid-foot. In the Pteropoda the
vring-hke swimming lobes (epipodia or pteropodia) corre-
spond to the two halves of the siphon, and are much the
largest element of the foot. The foro-foot surrounding
the head is often quite small, but in Clione and Pneumo^
dermon carries lobes and suckers. A hind-foot is in Ptero-
poda often distinctly present; it is open to doubt as to
whether the coixesponding region of the foot in Siphono-
poda is developed at alL
The lobes of the fore-foot of Nautilus and of the othes
Siphonopoda require further description. It has been
doubted whether these lobes were rightly referred (by
Huxley) to the fore-foot, and it had been maintained by some
zoologists (Qrenacher, Jhering) that they are truly processes
of the head. It appears tor the present writer to be im-
possible to doubt that the lobes in question are the fore-
portion of the foot when their development is examined
(see fig. 121, and especially fig. 72**), further, when the fact
is considered that they are innervated by the pedal-ganglion,
and, lastly, when the comparison of such a Siphonopod as
Sepia is made with such a Pteropod as Pneumodermon in its
larval (fig. 84) aswell as in its adult condition (fig. 85). The
Fio. 104. — Circulatory and excretory organs of Sepia (from GegenbaoT, after
John Hunter), hr, branchiae (ctenidia) ; e, yentricle of the heart ; a, anterior
artery (aorta) ; a", posterior artery ; v, the right and left aurtdes (enlargo-
menta of the efferent branchial veins) ; c', efferent branchial vein on the free
face of the gill-plume ; c.c, vena cava ; ri, vc", advehent branchial vessels
(blanches of the vena cava, see Qg. 106) ; vc", abdominal veins ; z, branchial
hearts and appendajges ; re- ^, glandular substance of the nephridia developed
on the wall of the great veins on their way to the gUlfl. ^e arrows Intlitat"
the direction of the blood-current.
larval Pneumodermon shows clearly that the sucker-bearing
processes of that Mollusc are originally far removed from
the head and close in position to the pteropodial lobes of
the foot. By differential growth they gradually embrace
and obliterate the head, as do the similar sucker-bearing
processes of Sepia. In both cases the sucker-bearing pro-
cesses are "fore-foot," The fore-foot of Nautilus completely
surrounds the buccal cone (fig. 88, «), so as to present an
appearance with its expanded tentacles similar to that of the
disc of a sea-anemone (Actinia). No figure has hitherto
been published exhibiting this circum-oral disc with its
tentacles in natural position as when the animal is alive and
swimming, the small figure of Valenciennes being deficient
in detail. All the publishsd figures represent the actual
appearance of the contracted spirit-epecimens. Mr A Q.
XVI. — 8s
674
MOLLUSCA
[cEPHAJUOPODl.
Bourne, B.Sc, of University College, has prepared from
actual specimens the drawings of this part in the male and
female Nautilus reproduced in fig.. 88, and has restored the
parts to their natural form when expanded. The drawings
show very strikingly the difference between male and female.
In the female (lower figure), we observe in the centre of
the disc the buccal cone e carrj'ing the beak-like pair of
jaws which project from the finely papillate buccal membrane.
Three tentaculiferous lobes of the fore-foot are in immediate
contact with this buccal cone ; they are the right and left
(c, <•) inner lobes, as we propose to call them, and the in-
ferior inner lobe ((/), — called inferior because it really lies
ventralwards of the mouth. • This inner inferior lobe is
clearly a double one, representing a right and left inner
inferior lobe fused into one. A lamellatcd organ on its sur-
face, probably olfactory in function (n), marks the separation
of the constituent halves of this double lobe. Each half
cari'ies a group of fourteen tentacles. The right and the
left inner lobes (c, c) each carry twelve tentacles. Ex-,
Pif). 1C5. — Diagram to show the relatlonfl of the heart In the MoUosca (from
GcgeDbauT). A. Part of the dorsal vascular trunk and transverse trunKs of
a worm. Xi. Ventricle and auriolos of Nautilus. C. Of a Lamellibranch, of
Chiton, or of Loligo. D. Of Octopus. E. Of a Gastropod, n, auricle ; v,
ventricle; oc, erteria cephallca (aorta): ai, aiLcria abdoininaliB. Ths arrows
show the direction of tlie blood-current.
ternal to these three lobes the muscular substance of the
mouth-embracing foot is raised into a wide ring, which
becomes especially thick and large in the dorsal region
where it is notably modified in form, offering a concavity
into which the coil of the shell is received, and furnish-
ing a protective roof to the retracted mass of tentacles.
This part of the e.xtemal annular lobe of the fore-foot is
called the "hood" (figs.. 90, 91, m.). The median antero-
posterior line traversing this hood exactly corresponds to
the line of concrescence of the two halves of the fore-foot,
which primitively grew forward one on each side of the
bead, and finally fused together along this line in front of
the mouth. The tentacles carried by the great annular
lobe are nineteen on each side, thirty-eight in all. They
are somewhat larger than the tentacles carried on the three
inner lobes. The dorsalmost pair of tentacles (marked
g in fig. 88) are the only ones which actually belong to
that part of the ih:o which forms the great dorsal hood m.
The hood is, in fact, to a large extent formed bythe enlarged
sheaths of these two tentacle,"!. In the Ammonites (fossi!
Tetrabranchiata allied to Nautilus) the dorsal surface of
the hood secreted a shelly plate in two pieces, known to
palfEontologists as Trigonellites and Aptychus. Possibly,
however, this- double plate was carried on the surface ot
the bilobed nidamental gland with the form and sculptur-
ing of which, in Nautilu.i, it closely agrees. All the ttn-
taclos of the circum oral disc are set in remarkable tubular
sheaths, into which they can bo drawn. The sheaths of
Eome of those belonging to the external or annular lobo are
«cou in fig. 91, marked n. The sheaths are muscular as
well as the tentacles, and are simply tubes from the base
of which the solid tentacle grows. The functional signifi-
cance of this sheathing arrangement is as obscure as it",
inorpliologiral origin. With ryferonce to the latter, it
■tppcars highly probable that the tubular sheath represents
the cup of a sucker such as is found on the fore-foot of the
Dibranchiata. In any case, it seems to the writer impos-
sible to doubt that each tentacle, and its sheath on a lobp
of the circum-oral disc of Nautilus, corresponds to a suckc
on such a lobe of a Dibranchiate. Keferstcin follows Owen
in strongly opposing this identification, and in regarding
such tentacle as the equivalent of a whole lobe or ami of a
Decapod or Octopod Dibranch. AVe find in the details of
these structures, especially in the facts concerning the
hectocotyliis and spadix, the most conclusive reasons for
dissenting from Owen's view. We have so far enumer-
ated in the female Nautilus ninety tentacles. Four more
remain which have a very peculiar position, and almost
lead to the suggestion that the eye itself is a modified
tentacle. These remaining tentacles are placed one above
(before) and one below (behind) each eye, and bring up
the total to ninety-four (fig. 91, v, v). They must be con-
sidered as also belonging to the fore-foot which thus sur-
rounds the eye.
In the adult male Nautilus we find the following im-
portant ditferences in the tentaculiferous disc as compared
with the female ' (see upper drawing in fig. 88). The
inner inferior lobe is rudimentary, and carries no tentacles.
It is represented by three groups of lamelbe (d), which are
not fully exposed in the drawing. The right and left inner
lobes are subdinded each into two portions. The right
shows a larger portion carrying eight tentacles, and smaller
detached groups (q) of four tentacles, of which three have
their sheaths united whilst one stands aloue. These four
tentacles may be called the "anti-spadix." The left inner
lobe shows a similar larger portion carrying eight tentacles,
and a curious conical body in front of it coiresponding to
the anti-spadix. This is the " spadix " of Van der Hoeven
(36). It carries no tentacles, but is terminated by imbri-
cated lamellae. These lamellae appear to represent the four
tentacles of the anti-spadix of the right internal lobe, and
are generally regarded as corresponding to that modification
of the sucker-bearing arms of male Dibranchiate Siphono-
pods to which the name " hectocotylus " is applied. The
spadix is in fact the hectocotylized portion of the fore-
foot of the male NautUus. The hcctocotylized arm or lobe
of male Dibranchiata is Connected with the process of copu-
lation, and in the maie Nautilus the spadLx has probably a
similar significance, though it is not possible to suggest
how it acts in this relation. It is important to observe
that the modification of the fore-foot in the mala as com-
pared with the female Nautilus is not confined to the
existence of the spadix. The anti-spadix and the reduction
of the inner inferior lobe are also male peculiarities. The
external annular lobe in the male does not differ from that
of the female ; it carries nineteen tentacles on each side.
The four ophthalmic tentacles are also present. Thus in
the male Nautilus we find altogether sixty-two tentacles,
the thirty -two additional tentacles of the female being repre-
sented by laraelliform structiu-es.
If we now compare the fore-foot of the Dibranchiata with
that of Nautilus, we find in the first place a more simple
arrangement of its lobes, which are either four or five pairs
of tapering processes (called " arms ") arranged in a series
around the buccal cone, and a substitution of suckers for
tentacles on the surface of these lobes (figs. 92, 95, 96)
The most dorsally-placed pair of arms, corresponding to the
two sides of the hood of Nautilus, ore in reality the most
anterior (sec fig. 75, (G) ), and ore termed the first pair. In
the Octopuda there are four pairs of those arms (figs. 94,
95), in the Decapoda five jiairs, of which the fourth is
greatly elongated (figs. 92, 93). In Sepia and other Deca-
poda (not all) each of these long arms is -n-ithdrawn into a
pouch beside the head, and is only ejected for the purpose
of prehension. The figures referred to show some of the
variations in form which these arms may assume. In the
CEPHALOPODA.]
MOLLUSCA
675
Octopoda tney are not unfreqnently connected by a web,
and form an efficient swimming-belL The suckers are placed
OK the ad-oral surface of the arms, and may be in one,
two, or four rows, and very numerous. In place of suckers
in some genera we find on certain arms' or parts of the
arms homy hooks ; in other cases a hook rises from the
centre of each sucker. The hooks on the long arms of
Onychoteuthis are drawn in fig. 97. The fore-foot, with
its apparatus of suckers and hooks, is in the Dibranchiata
essentially a prehensile apparatus, though the whole series
of arms in the Octopoda serve as swimming organs, and in
many (e.<?., the Common Octopus or Poulp) the sucker-
bearing surface is used as a crawling organ.
In the males of the Dibranchiata one of the arms is
more or less modified in connexion with the reproductive
function, and ia called the " hectocotylised arm." This
name is derived from the condition assumed by the arm
in those cases in which its modification is carried out to
the greatest extent. Thesa cases are those of the Octo-
pods Argonauia argo and Parasira caienvlata (fig. 9G).
In the males of these the third arm (on the left side in
Argonauta, on the right side in Parasira) is found before
the breeding season to be represented by a globular sac of
integument. This sac bursts, and from it issues an arm
larger than its neighbours, having a small sac at its extremity
in Parasira (fig. 96, x), from which subsequently a long
filament issues. Before copulation the male chaxges this
arm with the spermatophores or packets of spermatozoa
removed from its generative orifice beneath the mantle-skirt,
and during coitus the arm becomes detached and is left
adhering to the female by means of its suckers. A new arm
is formed at the cicatrix before the next breeding season.
The female, being much larger than the male, s-nims away
with the detached arm loHged beneath her mantle-skirt.
There, in a way which is not understood, the fertilization
of the eggs is effected. Specimens of the female Parasira
with the detached arm adherent were ezamiued by Cuvier,
who mistook the arm for a parasitic worm and gave to it
the name Hectocotylus. Accordingly, the correspondingly
modified arms of other Siphonopoda are said to be hecto-
cotylized. Steenstrup has determined the hectocotylized
condition of one or other of the arms in a nimiber of male
Dibranchs ts follows : — in all, excepting Argonauta and
Parasira, the laodincation of the arm ia slight, consisting in
a small enlargement of part or the whole of the arm, and-
the obliteration of some of its suckers, as shown in fig. 95,
A, Bj in Octopus and Eledone the third right arm is
hectocotylized; in Rossia the first left arm is hectocotylized
along its whole length, and the first right arm abo in the
middle only ; in Sepiola only the first left arm along its
whole length ; in Sepia it is the fourth left arm which is
modified, and at its base only ; in Sepioteuthis, the same at
its apex ; in Loligo, the same also at its apex; in Loliolus,
the same along its whole length ; in Ommastrephes,
Onychoteuthis, and Loligopsis no hectocotylized arm has
hitherto been observed.
In the females of several Dibranchs (Sepia, &c.) the
packets of spermatozoa or Eporiaatophores received from
the male have been observed adhering to the smaller arms.
How they are passed in this case by the female to the ova
in order to fertilize them is unknown.
Musculature, Fins^jxnd Cartilaginous Skeleton. — Without
entering into a detailed account of the musculatm-e of
Nautilus, we may point out that the great muscular masses
of the fore-foot and of the mid-foot (siphon) are ultimately
traceable to a large transverse mass of muscular tissue,
the ends of which are visible through the integument on
the right and left surfaces of the body dorsal of the
free flap of the mantle-skirt (fig. 89, I, I, and fig. 91, k).
These moscukr areie have a certain adhesion to the shell.
and serve both to hold the animal in its shell and as the
fixed supports for the various movepients of the teataculi-
ferous lobes and the siphon. Tbey are to be identified
with the ring-like asea of adhesion by which the f oot-muscia
of the Limpet is attached to the shell of that animal (see
fig. 27). In the Dibranchs a similar origin of the muscular
masses of the fore-foot and mid-foot from the sides of the
shell — modified, as this is, in position and relations — can be
traced.
In Nautilus there are no fin-like expansions of the integu-
ment, whereas such occur in the Decapod Dibranchs along
the sides of the visceral himip (figs. 92, 93). As an excep-
tion among Octopoda lateral fins occur in Pinnoctopus (fig.
94, A), and in Cirrhoteutbis (fig. 94, D). In the Ptero-
podous division of the Cephalopoda such fin-like expansions
of the dorsal integument do not occur, which is to be con-
nected with the fact that another region, the mid-foot^ which
in Siphonopoda is converted into a siphon, is in them
expanded as a pair of fins.
In Nautilus there is a curious plate-like expansion of
integument in the mid-dorsal region just behind the hood,
lying between that structure and the portion of mantle-
skirt which is reflected over the shell This is shown in
fig. 90, b. If we trace out the margin of this plate we
find that it becomes continuous on each side vrith the
sides of the siphon or mid-foot. In Sepia and other Deca-
pods (not in Gctopods) a closely similar plate exists in an
exactly corregponding position (see b in figs. 110, 111). In
Sepia a cartilaginous development occurs here immediately
below the integument forming the so-called " nuchal plate,"
drawn in fig. 116, D. The morphological significance of
this nuchal lamella, as seen both in Nautilus and in Sepia,»
is not obvious. Cartilage having the efracture shown in
fig. 117 occurs in various regions of the body of Siphono-
poda. In all Glossophorous Mollusca the lingual apparatus
is supported by internal skeletal pieces, having the char-
acter of cartilage ; but in the Siphonopodous Cephalopoda
such cartilage has a vrider range.
In Nautilus a large H-shaped piece of cartuaga is found
forming the axis of the mid-foot or siphon (£^. 116, A,
B). Its hinder part extends up into the head and supports
the peri-cesophageal nerve-mass (a), wliilst its two anterior
rami eictend into the tongue-like siphon. In Sepia, and
Dibranchs generally, the cartilage takes a different form,
as shown in fig. 116, C. The processes of this cartilage
cannot be identified in any Vay with those of the capito-
pedal cartilage of Nautilus. The lower larger portion of
this cartilage in Sepia is called the cephalic cartilage, and
forms a complete ring round the oesophagus ; it completely
invests also the ganglionic nerve-collar, so that all tha
nerves from the latter have to jjass through foramina in
the cartilage. The outer angles of this cartilage spread
out on each side so &s to form a cup-like receptacle for the
eyes. The two processes sprkiging right and left from this
large cartilage in the median line (fig. 116, C) are the
" prae-orbital cartilages ; " in front of these, again, there is
seen a piece like an inverted T, which forms a support to
the base of the "arms" of the fore-foot, and is the "basi-
brachial " cartilage. The Decapod Dibranchs have, further,
the " nuchal cartilage " already mentioned, and in Sepia, a
thin plate-like * 6ulM)Stracal " or (so-called) dorsal cartilage,
the anterior end of which rests on and fits into the concave
nuchal cartilage. In O'topoda there is no nuchal cartilage,
but two band-like " dorsal carrilascs." In Decapods there
are also two cartilaginous sockets on the sides of the funnel
— " siphon-hinge cartilages " — into which fleshy knobs of
tha mantle-skirt are loosely fitted. In Sepia, along the
whole base-line of each lateral fin of the mantie (fig. 92),
is a " basi-pterygial cartilage." It is worthy of remark th^vt
we have, thvs developed, in Dibrauch Siplionopods a morf,
676
MOLLUS'CA
[CEPILVLOPODA.
complete internal cartilaginous skeleton than is to be found
in some of tie lower Vertebrates. There are other instances
of cartilaginous endo-skeleton in groups other than the
Vertebrata. Thus in some capito-liranchiate Chxtopods
cartilage forms a skeletal support for tho giU-plmnes, whilst
in. the Arachnids (IVIygale, Scorpio) and in Limulus a large
internal cartilaginous plate— the ento-sternite — is devel-
oped as a support for a large series of muscles.
Alimentary Tract. — The buccal cone of Nautilus is ter-
minated by a villous margin (buccal membrane) .siu-round-
ing the pair of beak-like jaws. These are very strong and
dense in Nautilus, being calcified. FosdiliEed beaks of Tetra-
branchiata are known under the name of RhynchoHtes.
In Dibranchs the beaks are horny, but similar in shape to
thoSe of Nautilus. They resemble in general those of a
parrot, the lower beak being the
larger, and overlapping the upper or
dorsal beak. The Ungual ribbon and
odontophoral apparatas has the struc-
ture which is typical for Glosso-
phorous MoUusca. In fig. 107, A is
represented a single row of teeth
from the lingual ribbon of Nautilus,
and in fig. 107, B, C, of other Si-
phonopoda.
In Nautilus a long and wide crop
or dilated oesophagus {cr, fig. 110)
passes from the muscular buccal mass,
and at the apex of the visceral hump
passes into a highly muscular stom-
ach, resembling the gizzard of a bird
{gizz, fig. 110). A nearly straight
intestine passes from the muscular
stomach to the anus, near which it
develops a small ctecum. In other
Siphonopods the oesophagus is usually f,o. loc— Alimentary canal
narrower (fig. 106, oe\ and the mus- ofi^hjomjidaiactromGe
, \ o ) /» ^ Kenbaur) The buccal mass
cular stomach more capacious' (fig. is omitted »«, cEsophagiis .
106, .),_ whilst a very important :;^£T^T^,11ZVZI,
feature in the alimentary tract is through the pylorus; c,
c ji,iT, T 111., commencement of the c:e-
formed by the caecum. In all but cum ; t, its spiral portion ;
Nautilus the cscum lies near the \i «««''''=; f. '°'''>^? • ''■
, J , it6openingintotberecti:m
Btomacn, and may be very capacious
— much larger than the stomach in LoKgo vulgaris — ni'
■ elongated into a spiral coil, as '■' fig. 106. e. The simple
plicity in consequence of their visceral hump being un-
twisted. The acini of the large liver of Nautilus are
compacted into a solid reddish-brown mass by a firm
membrane, as also is the case in the Dibranchiata.
The Uver has four paired lobes in Nautilus, which open
by two bile-ducts into the alimentary canal at the com-
mencement of the intestine. The bile-ducts unite before
entering the intestine. In Dibranchiata the two large
lobes of the liver are placed antero-dorsally (beneath
the shell in Decapoda), and the bile-ducts open into the
cjecum. ' Upon the bile-ducts in Dibranchiata are deve-
loped yellowish glandulai' diverticula, which are known
as "pancreas," though neither physiologically nor morpho-
logically b there any ground for considering either the so-
called liver or the so-called pancreas as strictly equivalent
to the glands so denominated in the Vertebrata. In Nauti-
lus the equivalents of the pancreatic diverticula of the
Dibranchs can be traced upon the relatively shorter bile-
ducts.
Salivary Glands are not developed in Nautilus unless a
pair of glandular masses lying on the buccal cavity are to
be considered as such. In the Dibranchs, on the contrary,
one (Sepia, Loligo) or two pairs of large salivary glands
are present, an anterior and a posterior (Octopus, Eledone,
Onychoteuthis). Each pair of salivary glands has its
paired ducts united to form a single duct, which runs
forward from the glands and opens into the buccal cavity
'•y-
::-r^ni
Fto, 107.— Lln8:ual dentition of filphonopi-Kla.
of Kaiifilus pompiliiis (after Kofonstcln).
Stfiia oJJicinalM (after Trosc"
Loveo).
luir of linsTinl teeOi
of Uogiml tfMh of
Lingual te«th of Eledotu virriiosa (alter
l7-shapecl flexure of the alimentary tract aa c-ioen in fig.
106, and in fig. 110, is the only importuiit one which it
cxhibit-s in the Cephalopotia, — the Pteropoda (except the
Limaeinida) agreeing with the Siphonopoda in this siin-
nJ tho veins which nm through
, „ . rbe nephrldial sacs are eupposetl
to liave their upper walls removed, v.c, vena cava ; r.d.v.c, right descending
branch of tho same ; r.3.v.c, left descending bi-snch of the same ; v.b.a,, vein
fmni tho ir.k-bag ; v.vi, mesenteric vein ; v.g, genital vein ; v.a.d, riglit
abdominal vein ; v.a.s, loft abdominal vein ; v.p.d, right pallial vein ; v.p.K,
l--rt pullial vein ; c.h, branchial heart ; x, appendage of the same ; c.t>. capsule
I'f tlin branchial heart; np, external aperture of the right nephridial sac; (f,
rLTK-ppricardial orifice placing the left renal sac or nephridium in communi-
cali'iu with the vise ero- pericardial sac, the course of which below the nepkri-
ilial sac ia ibdicated by dotted lines ; j/", tho similar orifice of the right side ;
a.r, slandular renal outgrowtlis ; w.k, vlsccro- pericardial sac (dotted outlineX
near the radula. The anterior pair of glands when present
lie in the head near the buccal mass, the posterior pair lie
much farther back beneath the liver, at the sides of the
oesophagus.. It is the posterior pair which alone are pre-
sent in Sepia and Loligo. The ink-bag is to be considered
as an appendage of the rectum. It is not developed in
Nautilus, nor in the Pteropoda; in all Dibranchiata (even in
the fossil Belemnites) it is present (fig. 106, a ; fig. 103, (),
and has been observed to develop as a diverticulum of the
rectum, with spirally plaited walls which very early secrete
a binck pigment. The spiral plaitings of the walls diminish
CEPHALOPODA.]
MOLLUSCA
677
in relative size as the volume of the sac increases. Its
outer surface acquires a metallic iridescence similar to that
of the integuments of many fishes. The opening of the
ink-sac is in the adult sometimes distinct from but near to
Vto. 109.— Diagram to sliowthe relatione of nicfonrnephrldlal sacs, thoviacero-
pcricardial sac, and the heart and large vessels in Santilus (drawn by A G.
Bonme). neph, Mtph, on the right side point to the two nephridia of that
aide (the two of the opposite side are not lettered),- -each is seen to have an
Independent aperture ; j is the \iscero- pericardial sac, the dotted line indicat-
ing it3 backv-ard extension ; visc.per.apert marlcs an arrow introduced into
the right aperture of the viscero-pericardial sac; r.e., r.e.. point to the
glandular enlarged walls of the advehent hrancliial vessels, — two small
glandular bodies of the kind are seen to project into each nephridial sac.
whilst a larger body of the same kind depends from each of the four branchial
advelient vessels into tlie viscero-pei-icardial sac; v.c, vena cava; re»f,
ventricle of the heart; ao., ceplialic aorta (the small abdominal aorta not
draAvn) ; a.b.v, advehent branchial vessel ; c.v.b., efferent branchial vessel.
the anus (Sepia) ; in other cases it opens into the rectum
near the anus. The ink-bag of Dibranch Siphonopoda is
IKissibly to bo identified with the adrectal (purpuriparous)
gland of some Gastropoda.
Ccelom, Blood-vascular System, and Excretory Organs. —
Nautilus and the other Siphonopoda conform to the
The parts which are quite black ai% the cut muscular s'jrlaces of the foot and
buccal mass, a, the shell ; 6, the nuchal plate identical with the nuchal
cartihige of Sepia (see flg. 90, V) ; c, the integument covering the visceral
hump ; d, the mantle flap or skirt in the dorsal region where it rests against
the coil of the shell ; e, the inferior margin of the mantle.slcirt resting on the
lip of the shell represented by the dotted line ; /, the pallial chamber with
two of the four gills ; g, tlie vertically cut median portion of the mid-foot
(siphon); ft, the capito-pedal cartilage (see fig. 116); i, the valve of the
siphon : I, the siphuncular pedicle (cut short) ; m, the hood or dorsal enlarge,
mcnt of the annular lobe of the fore-foot ; n, tentacles of the annular loije ;
IS tentacles of the inner Inferior lobe : q, buccal membrane ; r, upper jaw or
beak : », lower jaw or beak ; t, lingual ribbon ; i, the viscero-pericarxlial sac ;
n.c, nerve-collar ; oe, oesophagus ; ct, crop ; gizz, gizzard ; i" 'i/, intestine ; an,
anus; iii, nidamental gland; ncpt, aperture of a nephridial sac; r.e, renal
glandulaj masses on the walls of the afferent branchial veins (see tig 109) ;
" ', efferent branchial vessel ; tf, ventricle
general Molluscan characters in regard to these organs.
Whilst the general body-cavity or coelom forms a lacunar
blood-system or series of narrow spaces, connected with
the trunks of a well-developed vascular system, that part
of the original coelom surrounding the heart and known
as the Molluscan pericardium becomes shut off from this
general blood-lymph system, and communicates, directly in
Nautilus, in the rest through the nephridia, with the exte-
rior. In the Siphonopoda this specialized pericardial cavitj-
is particularly large, and has been recognized as distinct
from the blood-carrjTjig spaces, even by anatomists who
have not considered the pericardial space of other Mollusca
to be thus isolated. The enlarged pericardium, which may
even take the form of a pair cf sacs, has been variously
named, but is best known as the viscero-pericardial sac or
chamber. In Nautilus this sac occupies the whole of the
postero-dorsal surface and a part of the antero-dorsal (see
fig. 110, x), investing the genital and other viscera which
lie below it, and having the ventricle of the heart sus-
pended ia it. Certain membranes forming incomplete
septa, and a curious muscular band — the pallio-cardiac
band — traverse the sac. The four branchial advehent veins,
which in traversing the walls of the four nephridial sacs
6i> e off, as it were, glandular diverticula into those sacs,
also give off at the same points four much larger glandular
app.
Tic. 111. — Diagram representing a vertical approximately median antero-
posterior section of Seyia o^cinalie (&om a drawing by A. O. Bourne). Tbe
lettcringcorresponds with that of fig. 110, ivith which this drawing is intended
to be compared, a, aheU (here enclosed by a growth of the mantle); 6, the
nuclial plate fhere a cartilage); c (the reference line should be continued
through the black area rep|esentinfi the shell to the outline below It), the
integujnent covering the \nsceral hump ; d, the reflected portion of the
mantle-skirt forming the eac which encloses the sheU ; e, the inferior margin
of the mantle-skirt (mouth of the pallial chamber) ; / the paUial chamber ;
g, the vertically cut median portion of the mid-foot (siphon) ; (, the valve oi
the siphon : m, the two opper lobes of the fore-foot ; n, the long prebensnc
arms of the saioe ; o, the fifth or lowermost lobe of the fore-foot ; p, the third
lobe of tlie fore-foot ; 5, the buccal membrane ; v, the opper beak or jaw ;_«,
the lower besk or jaw ; f, the lingual ribbon ; z, the viscero-pericardial sac ;
n.c, the nerve-collar ; cr., the crop ; gizz., the gizzard ; an, the anus ; c.(., the
left ctenidiujn or gill-plume; vent, ventricle of the heart; a.b.v., affereat
branchial vessel ; t.b.v, efferent brancliial vessel ; re, renal glandular mass ;
n.n.a, left nephridial apei-ture; visc.per.apert. , viscero-pericardial aperture
(see fig. IDS) ; br.b., branchial heart ; opp., appendage of the same ; i.s., Ink-
bag.
masses, which hang freely into the viscero-pericardial
chamber (fig. 109, r.e). In Nautilus the viscero-pericardial
sac opens to the exterior directlj' by a pair of apertures, one
placed close to the right and one close to the left posterior
nephridial aperture (fig. 101, viscper.). This direct opening
of the pericardial sac to the exterior is an exception to what
occurs in all other Mollusca. In all other Molluscs the
pericardial sac opens into the nephridia, and through them
or the one nephridium to the exterior. In Nautilus there
is no opening from the viscero-pericardial sac into the
nephridia. Therefore the external pore of the viscero-peri-
cardial sac may po.^ibly be regarded as a shifting of _ the
reno-pericardial orifice from the actual wall of the nephridial
sac to a position alongside of its orifice. Parallel cases
of such shifting are seen in the varying position of the
orifice of the ink-bag in Dibranchiata, and in the orifice
of the genital ducts of Mollusca, which in some few cases
(e.g., Spondylus) open into the nephridia, whilst in other
cases they open close by the side of the nephridia on the
surface of the bodv. The viscero-nericaidl-Ll sac "f tUt
678
M O L L U S C A
[cephalopoda.
Dibranchs b very large also, and extends into the dorsal
region. It varies in shape — that is to say, in the extensions
of its area right and left between the various viscera, — in
different genera, but in the Decapods is largest. In an ex-
tension of this chamber is placed the ovary of Sepia, whilst
the ventricle of the heart and the branchial hearts and their
appendages also lie in it. It is probable that water is
drawn into this chamber through the nephridia, since sand
and other foreign matters are found in it. In all it opens
into the pair of nephridial sacs by an orilice on the wall of
each, not far from the external orifice (fig. 108, y, y').
There does not seem any room for doubting that each orifice
corresponds to the reno-pericardial orifico which we have
seen in the Gastropoda, and .shall find again in the Lamelli-
branchia. The single tube-lilce nephridium and the peri-
eardirju of the Pteropoda also communicate by an aperture.
The circulatory organs, blood-vessels, and blood of Nauti-
lus do not difiTer greatly from those of Gastropoda. The
ventricle of the heart is a four-cornered body, receiving a
dilated branchial eifertnt vessel (auricle) at each comer
(fig. 103). It gives off a cejihalic aorta anteriorly, and
a smaller abdominal aorta posteriorly. The diagram, fig.
105, serves to show how this simple form of heart is related
to the dorsal vessel of a worm or of an Artliropod, and how
by a simple flexure of the ventricle (D) and a subsequent
suppression of one auricle, following on the suppression of
one brancMaJ~one may obtain the form of heart charac-
teristic of the Anisopleurous Gastropoda (excepting the
Zygobranchia). The flexed condition of the heart is seen
in Octopu.'i, and is to some extent ap^.roached by Nautilus,
the median vessels not presenting that perfect parallelism
which is shown in the figure (B). The most remai-kable
feature presented by the heart of Nautilus is the possession
of four instead of two auricles, a feature which is simply
related to the metamerism of the branchiae. By the left
side of the heart of Nautilus, attached to it by a membrane,
and hanging loosely in the viscero-pericardial chamber, is
th? pyriform sac of Owen. This has recently been shown
to bo the rudimentai'y left oviduct or sperm-duct, as the
case may be (Lankester and Bourne, 37), the functional
right cvi-sac and its duct being attached by a membrane
to the opposite side of the heart.
The cephalic and abdominal aortse of Nautilus appear,
after running to the anterior and posterior extremes of the
animal respSctively, to open into sinus-like spaces surround-
ing the viscera, muscular masses, <fcc. These spaces are
not large, but confined and shallow. Capillaries are stated
to occur in the integument. In the Dibranclis the arterial
system is very much more complete ; it appears in some
cases to end in irregular lacunie or sinuses, in other cases
in true capillaries which lead on into veins. An investiga-
tion of these capillaries in the light of modern histological
knowledge is much needed. From the sinuses and capil-
laries the veins take origin, collecting into a large median
trunk (the vena cava), which in the Dibranchs as well as in
Nautilus has a ventral (postero-ventral) position, and runs
parallel to the long axis of the animal. In Nautilus this
vena cava gives off at the level of the gills four branchial
advehent veins (fig. 109, v.c), which pass into the four
g^la OTthout dilaticg. Li the Dibranchs at a similar posi-
tion tho vena cava gives off a right and a left branchial
advcheat vein (fig. 108, r.s.v.c, r.d.v.c), each of which,
traversing the wall of tho correviponding nephridial .Siic and
receiving additional factor^ (fig. 108, v.(j, v.p.d, v.a.d, v.b.a),
dilates at the base of the corresponding branchial plume,
forming there a pulsating sac — the branchial heart (fig.lOi,
x; and Uti 108, c.h). Attached to each branchial heart is a
cttfious glandular body, which may possibly be related to
ths larger ma-ss?s (r.c in fig. 109) which depend into tho
viscero-pericardial cavity from tho branchial advehent veins
of Nautilus. From the dilated branchial heart the bran-
chial advehent vessel proceeds, running up the ad-pallial
face of the gill-plume {vi, vc',, fig. 104). From each gill-
plume the blood passes by the branchial efferent vessels
(v, fig. 104) to the heart, the two auricles being formed
by the dilatation of these vessels (a, v in fig. 104).
The blood of Siphonopoda contains the usual amoeboid cor-
puscles, and a diffused colouring matter — the haemocyanin
of Fredericque — which has been found also in the blood of
Helix, and in that of the Arthropods Homarus and limulns.
It is colourless in the oxidized, blue in the deoxidized state^
and contains copper as a chemical constituent.
The nephridial sacs ^cljenal glandular tissue are closely
connected ivith the branchial advehent vessels in Nautilus
and in the other Siphonopoda. The arrangement is snch
0^ to render the typical relations and form of a nephridium
difficult to trace. In accordance with the metamerism of
Nautilus already noticed, there are two pairs of nephridia.
Kach nephridium assumes the form of a sac opening by a
pore to the exterior. As is usual in nephridia, a glandiilar
and a non-glandular portion are distinguished in each sac ;
these portions, however, are not successive parts of a tube, as
happens in other cases, but they are localised are33 of the wall
of the sac. The glandular renal tissue is, in fact, confined
to a tract extending along that part of tho sac's wall which
immediately invests the great branchial advehent voin.
The vein in this region gives off directly from its wall a
complete herbage of little venules, which branch and ana-
stomose with one ar.other, and are clothed by tho glandular
epithelium of the nephridial sac. The secretion is accumu-
lated in the sac and passed by its aperture to the exterior.
Probably the nitrogenous excretory product is very rapidly
discharged ; in Nautilus a pink-coloured powder is found
accumulated in the nephridial sacs, consisting of calcium
phosphate. The presence of this
phosphatic calculus by no means
proves that such was the sole ex-
cretion of the renal glandular tis-
sue. In Nautilus a gLandtilar
growth like that rising from tho
wall of the branchial vessel into
its corresponding nephridial sac,
but larger in size, depends from
each branchial advehent vessel into
the viscero-pericardial sac, — prob-
ably identical with the "append-
age" of tho branchial hearts of
Dibranchs.
The chief difference, other than
that of number between tho ne-
phridia of the Dibranchs and those
of Nautilus, is the absence of the
accessory growths depending into
the viscero-pericardial space just
mentioned, and, of more import-
ance, the presence in the former of p,„ n'— '«j
a pore leading from the nephridial A'a«!iii« ;)c« .
sac into the viscero-pericardial sac ^^lon'-ifiM^S^gementJjoa
(v, y' in fi-.'. 108). The external nerves passing trom tho pcOoi
'/! r ?• 1. -J- I fanglion to the inner soncs of
orinces Ot tno nephridia are also tentacles; C, nerves to the ten-
yiore prominent in Dibranchs than Jj^- 1[ ^L°"^n°;„rpS
in Nautilus, being raised on iiapillaj «, cerebral gtngUon.riir); a,
(np in fig. 108 ; r in fig. 103). In &;S^ft,sT?SLi ^/IS
Sepia, according to Vigelius (38), "'f?."^''"^;^"':^^'^"''*'
tho two nephridU give off each nftl"olaij;evisceiul nerve, just
a diverticulmn dorsalwards, ^vhich ^!i"-Si*„tSafili^'Sri^
unites with its fellows ai.-.d forms "S nerves from tlio pleond
a great median renal chamber, e^eiion to the mantie-akirt.
lying between the ventral portions of the nephridia and
the viscero-. pericardial chamber. In Loligo the fusion
OEFBAXX>I>ODA.J
MOLLUSCA
679
of the two nepliridia to form one sac ia still more obvions,
since the ventral portiona are united. In Octopus the
nephridia are quite separate.
Tegumental pores have not been described in Nautilus,
but exist in Dibranchiata, and have been (probably
erroneously, but further investigation is needed) supposed
to introduce water into the vascular system. A pair of
Fig. 113.
Fig. 114.
Fiaa lis, 114.— Nerve^sentrta of Octopna, Figon 118 givM a rltwtrma the
dOTWl aspect, flfore 114 one from the ventnl opect. &u«, the buccal maM ;
jKd, pedal gan^on ; opt, optic ganglion ; oar, cerebral ganglion ; p4 pleural
ganglion ; piscj Tteoeial g«}gl]on ; as, cesopbagna ; / foramen In the nerre-
D-..ias formed oj pedal, plenral, and vlscaiu gangUou-paira, traversed by a
biood-TCs^el.
such pores leading into sub-tegmnental spaces of consider-
able area, the nature of which is imperfectly known, erist
on the back of the head in Philonexis, Tremoetopus, and
Argonauta. At the base of the arms and mouth four such
pores are found in Histioteuthis and Ommastrephes, six
in Sepia, LoUgo, Onychoteuthis. Lastly, a pair of such
pores are found in the
Decapoda at the base
of the long arms, lead-
ing into tin extensive
sub -tegumental pouch
on each side of the head
into which .the long
arms can be, and usually
are; withdrawn. In
Sepia, Sepiola, and Boa-
sia the whole arm is
coiled up in these sacs ;
in Loligo only ^ part
of it is so; in Histio-
teuthis, Ommastrephes,
and Onychoteuthis, the
sacs are quite small
and do not admit the
arm;!.
Neroofus System. —
Nautilus, like the other J^i
Cephalopoda (e. jr., Pneu- "^2^.
modermon, fig. 87 ;
Octopus, fig. 113), ex-
hibits a great concentra-
tion of the typical Mol- „ .,, _^ , . ,„ .
, 1 ■ t Fio- 116.— Lateral view of the nervotis centres
lUSCan ganglia, as sno-vvn and nerves of the right side of OctopM ml-
in fie. 112. The ean- f"r<«(liomadrawingbyA.(J.Bom-ne). Ij,
. o , JIM buccal ganglion; cfr., cereoral ganglion;
glia take on a band-like p^., pedal ganglion ; pL, pleural, and vix.,
fA*». n*.^ «.u. V..4. i:4^t» visceialregionofthepleuro-visceralcanglioa;
form, and are but little ,an,. atlf, the right steUdte gangllSn If the
differentiated from their mantle connected by a nei-re to tho ple'Jral
J portion ; nxisc., the right viacertil nerve ;
commissures ana con- «.»;/, its (probably) olfactory branches;
nectives, — an archaic "•'^■' "^ hrafchiai branches.
condition reminding us of Chiton. The special optic out-
growth of the cerebral ganglion, the optic ganglion (fig.
112, o), ia characteristic of the. big-eyed Siphonopoda.
Hie cerebral ganglion-pair (a) lying above the oesophagus
is connected with two snb-cSSophageal ganglion-pairs of
band-like form. The anterior of these is the pedal 6. b,
and supplies the fore-foot with nerves i, t, as also the
mid-foot (siphon). The hinder band is the visceral and
pleural pair fused (compare fig 112 with fig. 87, and
especially with the typiral Euthynearons nervous system
of LinmEeus, fig. 22) ; from its pleural portion nerves pass
to the mantle, from its visceral portion nerves to the
branchiae and genital ganglion {d ia fig. 112), and in
immediate connexion with the latter is a nerve to the
osphradium or olfactory papilla. No buccal ganglia have
been observed in NautUus, nor has an enteric nervous system
been described in this animal, though both attain a special
development in the Dibranchiata, The figures (114 and
115) representing the nerve-centres ^ef Octopus serve to
exhibit the disposition of these parts in the Dibranchiata.
The ganglia are more distinctly sfvollen than in Nautilus.
In Octopua an infra^buccal gangUon-pair are present cor-
responding to the buccal gangiion-pair of Gastropoda. In
Decapoda a supra-buccaj ganglion-pair connected with
these are also developed. Instead of the numerous radi-
ating pallial nerves of Nautilus, we have in the Dibran-
chiata on each side (right and left) a large pleural
erve passing from the pleural portion of the pleuro-
viscertd ganglion to the mantle, where it enlarges to
form the steUate ganglion. From each stellate ganglion
nerves radiate to supply the powerful muscles of the
mantle-skirt. The nerves from the visceral portion of the
pleuro-visceral ganglion have the same course as in Nautilus,
but no osphradial papilla ia present. An enteric nervous
system is richly developed in the Dibranchiata, connected
with the somatic nervous centres through the buccal
ganglia, as in the Arthropoda through the stomato-gastric
ganglia, and anastomosing with deep branches of the vis-
ceral nerves of the viscero-pleural ganglion-pair. It has
been especially described by Hancock (39) in Opun»-
strephes. Upon the stomach it forms a single large and
readily-detected gastric ganglion. It is questionable as to
how far this and the " cava! ganglion " formed in some
Decapoda by branches of the visceral nerves which accom-
pany the vena cava are to be considered as the equivalents
of tie "abdominal ganglion," which in a typical Gastropod
nervous system lies in the middle of the visceral nerve-loop
or commissure, having the right and left visceral ganglia
on either side of it, separated by a greater or less length
of visceral nerve-cord (see figs. 20, 21, 22). There can be
little doubt tliat the. enteric nervous system is much more
developed in the Dibranchiata than in other MoUusca, and
that it effects a fusion with the typical '' visccfal '.' cords
more extensive than obtains even in (Jastropoda, where
such a fusion no doubt must also be admitted.
Special Sense-Organs. — Nautilus possesses a pair of
osphradial papUlse (fig. 101, olf) corresponding in position
and innervation to Spengel's organ placed at the base of the
ctenidia (branchiae) in all classes of MoUusca. This organ
has not been detected in other Siphonopoda. In Ptero-
poda it is well developed as a single ciliated pit, although
the ctenidia are in that group aborted (fig. 87, Osp.).
Nautilus possesses other olfactory organs in the region
of the head. Just below the eye is a small triangular
process (not seen in our figures), ha^iag the structure of a
shortened and highly-modified tentacle and sheath. By
Valenciennes, who is followed by Keferstein, this is regarded
as an olfactory organ. The large nerve which runs to this
organ originates from the point of juncture of the pedal
with the optic ganglion. The lamelliform organ upon the
inner inferior tentacular lobe of Nautilus is possibly also
olfactory in function. In Dibranchs behind the eye is e,
pit or open canal supplied by a nerve corresponding in
origin to the olfactory nerve of Nautilus above mentioned.
680
MOLLUSCA
[cephalopoda.
Possibly the sense of taste resides In certain processes
witbia the mouth of Nautilus and other Siphonopoda.
K ^^^
1-^
%.
the pedal portion of the nerve^rentrvj. 6. Lattral view "of the
laige anterior processes are sunk in the muscular anlistance of the siphon.
C. Cephalic cartilages of &pia offxinalU. D. Nuchal cartilage ot Sepia o^ici-
nalis.
The otocysts of Nautilus were discovered by Macdonalc.
(40). Each lies at the side of the head, ventral Oi
the eye, resting on the capito-pedal cartilage, and supported
by the largo auditory
nerve which arises
from the pedal gan- ^^
glion. It has the ^'
form of a small sac, 5; '
1 to 2 mm. in dia- /, ^ *
meter, and contains "^1
whetstone - shaped 'i
crystals, such as are ^
known to form the
otolitha of other Mol- ^ .
lusca. The otocysts
of Dibranchiata are
larger and deeply
sunk in the cephalic
cartilage. It has Fio. 117.— MInnta stmcturo of the cartilflBO of
been shown by Lan- I^"e<> C™"?. Gegenbaur after Furbnnger). a,
^ -r J simple, 6, dividing, cells ; c, canaliciui ; a, an
kester that they de- emptycartilage capsule with Jta pores ; s,canali-
velop as open pits '^'"' i° »-=="™-
(fig. 121, (5), (6), o), which gi-adually close up, the com-
munication with the exterior becoming narrowed into a
fine canal, which is reflected over one end of the sac, and
finally has its external opening obliterated. A single
otolith only Ls found in all Dibranchiata.
The eye of Nautilus is among the most interesting struc-
tia-es of that remarkable animal. No other animal which
has the same bulk and general elaboration of organization
has so simple an eye as that of Nautilus. When looked
at from the sui-face no metallic lustre, no transparent
coverings, are presented by it. It is simply a .slightly pro-
jecting hemispherical box like a kettle-drum, half an inch
in diameter, its surface looking like that of the surrounding
integument, whilst in the middle of the drum-membrane is
a minute hole (fig. 91, u). Owen very naturally thought
that some membrane had covered this hole in Ufo, and had
been ruptured in the specimen studied by him. "It, how-
ever, appears from the researches of Ileusen (41) that the
hole is a normal aperture leading into the globe of the eye,
(which is accordingly filled by sea-water during life. There
is no dioptric apparatus in Nautilus, and in place of refract-
iag lens and cornea "we have actually hero an arrangement
for forming an image on the principle of "the pin-hole
camera." There is no other eye known in the whole animal
kingdom which is 90 constructed. The Vr'alJ of the eye-
globe is tough, and the cavity is lined solely by the naked
retina, which is bathed by sea-water on one surface and
receives the fibres of the optic nerve on the other (see fig.
118, A). As in other Siphonopods (e.g., fig. 120, Ei, Re,
p), the retina consists of two layers of cells separated by a
layer of dark pigment The most interesting consideration
connected with this eye of Nautilus is found when the
further facts are noted — (1) that the elaborate lens-bearing
eyes of Dibranchiata pass through a stage of development
in which they have the same structm'e as the eye of Nautilus
— namely, are open sacs (fig. 119); and (2), that amongst
other MoUusca examples of cephalic eyes can be found which
in the adult condition are, like the eye of Nautilus and the
developing eye of Dibranchs, simple pits of the integument,
the cells of which are surrounded by pigment and connected
with the filaments of an optic nerve. Such is the structuro
C Z' .
Far ^
Co ep
Co \
)<^ -CS^s- ^'" r.,
A M
G.op
^ cp
Pio. 118.— 1
Patella).
(Oigopsid). /"ai, eyelid (outermost fold) ; Co, cornea (second fold) ; /r, '
(third fold) : /ji(l, 2, 3, 4, different parts of the integument ; I, deep portion
of the lens; J-, outer portion of the lens; Co.cp, ciliary body; Jt, retina;
N.trpy optic nerve ; Cop, optic ganglion ; x, inner layer of the retiiia ; if.5,
nervoua stratum of the retina. (From Balfour, after Grenacher.)
of the eye of the Limpet (Patella) ; and in such a simple eye
we obtain the clearest demonstration of the fact that the
retina of the Molluscan cephalic eye, like that of the
Arthropod cephaUc eye and unlike that of the Vertebrate
myelonic eye, b essentially a modified area of the general
epiderm, and that the sensitiveness of its cells to the action
of light and their relation to nerve-filaments is only a
specialization and intensifying of a property common to the
whole epiderm of the surface of the body. "What, however,
strikes us as especially reniarknble is that the simple form
of a pit, which in Patella serv.-i to accumulate a secretion
which acts as a refractive body, should in Nautilus be
glorified and raised to the dignity of an efficient optical
apparatus. Natural selection has had an altogether excep-
tional opportunity in the ancestors of Nautilus. In all other
MoUusca, starting as we may suppose from the foUicular or
pit^Uke condition, the eye has proceeded to acquire the form
of a dosed sac, the cavity of the closed vesicle being then
filled partially or completely by a refractive body (lens)
secreted by its walls (fig. 118, B). This is the condition
attained in most Gastropoda. It presents a striking contrast
to the simple Ai'thropod eye, where, in consequence of the
existence of a dense exterior cuticle, the eye does not fonn
a vesicle, and the lens is always part of that cuticle.
In the Dibranchiate division of the Siphonopoda the
greatest elaboration of the dioptric apparatus of the eye
is attained, so that we have in one sul>-class the extremea
of the two lines of development of the Molluscan eye, those'
two lines being the punctigerous and the lentigerous. The
structure of the Dibranchiate's eye is shown in section in figJ
118, C, and in fig. 120, and its development in fig. 1 19 and
fig. 123. The open sac which forms the retina of the young
Dibranchiate closes up, and constitutes the posterior ehambei!
of the eye, or primitive optic vesicle (fig. 123, h^jioi:). The
CKPHAIXjroDA.]
3I0LLUSCA
681
lens forms as a stractureless growth, projecting inwards from
the front -wall of this vesicle (fig. 1 23, B, I). The integument
around the primitive optic vesicle which has sunk below
A
Pro. 119. — Diagrams of scotioni thowicg the early stage of development 6f Mi«
eye of Loljgo when It is, like the permanent eye of Nautilus and of Patella,
an open sac. A. First appearance of the eye as a ring-like upgrowth. B.
Ingrowth of the ring-like wall so as to form a sac, the priiuitiTe optic vesicle
of Loligo. (From Laiikester.*
the surface now rises up and forms firstly nearest the axis
of the eye the iridian folds (if in B, fig. 123 ; ik in fig. 120 ;
Tr in fig. 118), and then secondly an outer circular fold
grows up like a wall and completely closes over the iridian
folds and the axis of the primitive vesicle (fig. 120, C).
This covering is transparent, and is the cornea. In the
oceanic Decapoda the cornea does not completely close,
but leaves a central aperture traversed by the optic axis.
These forms are termed Oigopsid£e by d'Orbigny (43), whilst
the Decapoda ■n-ith closed cornea are termed Myopsidse.
In the Octopoda the cornea is closed, and there is yet
another fold thrown over the eye. The skin surrounding
the cornea presents a free circular margin, and can be drawn
over the surface of the cornea by a sphincter muscle. It
thoa acts as an adjustable diaphragm, exactly similar in
Fio. 120.— HoTliont«l section of the eye of .Sepia (Ilyopsid). KK, cephalic
cartilages (see flg. 116) ; C, cornea (closed) ; i, Ions ; ci, ciliary body ; J?(
internal layer of the retina ; J!e. oitemal layer of the retina ; p, pigment
between these ; o, optic nerve ; 170, optic ganglion ; t and .'-■', cap.iular cartilage ■
It, cartilage of the iris ; to, white body ; m, argtrntiiie Inlegament. (Fi-om
Gegenbanr, after Hensen.)
movement to the iris of Vertebrates. Sepia and allied Deca-
pods have a horizontal lower eyelid, that is to say, only
one-half of the sphincter-like fold of integument is movable.
The exact history of the later growth of the lens in the
Dibranchs' eye is not clear. As seen in fig. 120, it appears,
after attaining a certain size, to push through the front
wall of the primitive optic vesicle at the point correspond-
ing to its centre of closure, and to project a little into the
anterior chamber formed by the cornea. The wall of the
primitive optic vesicle adjacent to the embedded lens (L)
now becomes modified, forming a so-called "ciliary body,;'
in which muscular tissue is present, serving to regulate tlw
focus of the lens (ci in fig. 120). Bobretzky (43) differs
from Lankester, whose view is above given, in assigning a
distinct origin to the protruding anterior segment of the
lens (l'- in fig. 118). The optic ganghon, as well as the
other large ganglia of the Dibranchiata, originate in the
mesoblast of the embryo. The connexion between the cells
of the retina and the nerve-fibres proceeding from the optic
ganglion must therefore be a secondary one.
Chromatopkores. — In Nautilus these remarkable struc-
tures, which we mention here as being intimately asso-
ciated with the nervous system, appear to be absent. In
Dibranchiata they play an important part in the economy,
enabling their possessor, in conjunction with the discharge
of the contents of the ink-bag, to elude the observation of
either prey or foe. They consist of large vesicular cells
(true nucleated cells converted into vesicles), arranged in
a layer immediately below the epidermis. Each chronia-
tophore-cell has from six to ten muscular bands attached
to its walls, radiating from it star-wise. The contraction
of these fibres causes the chromatophore-cell to widen
out ; it returns to its spherical resting state by its owTi
elasticity. In the spherical resting state such a cell may
measure '01 mm., whilst when fully stretched by its radiat-
ing muscles it covers an area of '5 mm. The substance
of the chromatophore-cells is intensely coloured with one
of the following colours — scarlet, yellow, blue, brown —
which are usually of the greatest purity and brilliance. The
action of the chromatophores may bft Wfttched most readily
in young Loligo, either under the microscope or with the
naked eye. The chromatophores are suddenly expanded,
and more slowly retracted with rapidly-recurring alter-
nation. All the blue, or all the red, or all the yellow
may be expanded and the other colours left quiescent.
Thus the animal can assume any particular hue, and
change its appearance in a dazzling way with extraordinary
rapidity. There is a definite adaptation of the colour
assumed in the case of Sepia and others to the colour of
the surrounding rock and bottom.
Gctiads and Genital Ducts. — In Nautilus it has recently
been shown by Lankester and Bourne (37) that the genital
ducts of both sexes are paired right and left, the left duct
being rudimentary and forming the " pyriform appendage,"
described by Owen as adhering by membranous attach-
ment to the ventricle of the heart, and shown by Kefer-
stein to communicate by a pore with the exterior. Thus
the Cephalopoda agree with our archi-Mollusc in having
bilaterally symmetrical genital ducts in the case of the
most archaic member of the class. The ovary (female
gonad) or the. testis (male gonad) lies in Nautilus as in
the Dibranchs in a distinct cavity walled ofif from the
other viscera, near the centro-dorsal region. This chamber
is formed by the ccelomic or peritoneal wall; the space
enclosed is originally part of the coelom, and in Sepia
and Loligo is, in the adult, part of the viscero-pericardial
chamber. In Octopus it is this genital chamber which
communicates by a right and a left canal with the nephrid-
ium, and is the only representative of pericardium. The
ovary or testis is itself a growth from the inner wall of this
chamber, which it only partly fills. In Nautilus the right
genital duct, v/hich is functional, is a simple continuation
to the pore on the postero-dorsal surface of the membran-
ous walls of the capsule in which lies the ovary or the
testis, as the case may be. The gonad itself appeara to
represent a single median or bilateral organ.
The true morphological nature of the genital ducts of the
Cephalopoda and of other Mollusca is a subject which invites
speculation and inquiry. In all the cases in which such
XVL — 86
882
M O L L U S C A
[cRPHAiOPODA.
ducts continuous with the tunic of the gonad itself occur —
viz., in Nematoid worms, in Arthropoda, and in Teleostean
fiKhes, besides Molluscii — there is an absence of definite
knowledge as to the mode of development of the duct.
It seems, however, from such facts as have been ascer-
tained that the gonad lies at first freely in the coelom,
and that the duct develops in connexion with the genital
note, and attaches itself to the embryonic gonad, or to the
capsule which grows around it. Tha question then arises
as to the nature of the pore. In other groups of animals
we find that the pore, and funnel or tube connected with
it by which the genital products are conveyed to the
exterior, is a modified ncphridium (usually a pair, one
right and one left). Is it possible that this is also the
case where the duct very early becomes united to the
gonad, and even gives rise to the appearance of a tubular
ovary or testis 1 Probably this is the case in Teleostean
fishes (see Huxley's observations on the oviducts of the
amelt, 44) ; but it seems to be a tenable position that in other
cases, including the MoUusca, the genital pore is a simple
opening in the body-wall leading into the body-cavity
or coelom, such as we find on the dorsal surface of the
earth-worm, which has become specialized for the extrusion
of the genital products. Possibly, as in Nemertine and
Chsetopod worms, the condition preceding the development
of these definite genital pores was one in which a temporary
rapture of the body-wall occurred at the breeding season,
and this temporary aperture has gradually become perma-
nent. The absence of genital pores in Patella, and some
Lamellibranchs which make use of the nephridia for the
extrusion of their genital products, suggests that the very
earliest Mollusca or their forefathers were devoid of genital
ducts and pores. In no MoUusca, however, is the nephrid-
ium used in the same way as a genital duct as it is in the
Chastopoda, the GephjTaea, and the Vertebrata ; for the
open mouth of the nuphridium in Mollusca leads into the
pericardial space, and it is not through this space and this
mouth that the genital products of any Mollusca enter
the nephridiuni (except perhaps in Neomenia), although
it is by this mouth that the genital products enter the
nephridium in the former ■ classes above named. Hence
the arrangement in Patella, &c., is to be looked, upon as a
special development from the simpler condition when the
Mollusca brought forth by rupture ( = schizodinic, from wSi's,
travail), and not as derived from the common arrangement
of adaptation of a nephridium to the genital efTcrent func-
tion ( = nephrodinic).'
The functional oviduct of Nautilus fo;-ms an albumini-
parous gland as a diverticulum, which appears to corre-
spond to a dilatation in the male duct, which succeeds the
testis itself, and is called the "accessory gland." The male
duct has c second dilatation (Needham's sac), and then is
produced in the form of a large papUla. In Dibranchs
the genital ducts are but little more elaborated. They are
ciliated internally. In female Octopoda, in Omraastrephes,
and in one male Octopod [EUdoiie moschata) the genital
ducts are paired, opening right and left of the anus. But
in all other Dibranchs a single genital duct only is deve-
loped, viz., that of the left side, and leads from the genital
capsule or chamber of the gonad to an asymmetrically-placed
pore. In the male Dibranchs the genital duct is coiled
and provided with a series of glandular dilatations and
* Cffilomate animnls are, acconiing to this nomenclature, either
Schizodinic or Porodinic The Porodinic group is divisible into Ne-
phrodinic and Idiodinic, in tlio former the nephridium serving as n
pore, in the latter a fipeci.al (fSioj) pore being developed. In each of
those latter groups the pore may be — (1) devoid of a duct, (2) provided
»iLh a duct which is unattached to the gonad and opens into the body-
CRvity, (3) provided with a duct which fuses with the gonad. Tlio
genital ducts of Idiodinic forms may be called Idiogonaducts, as dis-
Ifaiguisbed £ro& the Nephrogonaductt of nephrodiiiic forms.
receptacles. These are connected with the formation of
the Bpermatophores. In the Siphonopoda the spermatic
fluid does not flow as a liquid from the genital pore, but
the spermatozoa are made up into little packets before
extrusion. In other Mollusca (Pulmonata) and in oiher
animals (Chsetopoda) this formation of " sperm-ropes " is
known, but in the Siphonopoda it attains its highest
development. Exceedingly complicated structures of a.
cylindrical form (sometimes an inch in length) are foimed
in the male genital duct by a secretion which embeds and
cements together the spermatozoa. They are formed in
Nautilus as well as in Dibranchs, the actual manner in which
their complicated structure is produced being not easily con-
jectured. Accessory glands not forming part of the oviduct,
but furnishing the material for enclosing the eggs in an elastic
envelope, are found as paired structures, opening soma way
behind the anus in Nautilus (101, ff.n.) and in the Di-
branchs. They are known as the nidamental glands. In
the female Sepia they are particularly large and prominent,
and are accompanied by a second smaller pair.
Rejrroductimi and Develojmieni. — The details of sexual
congress and of the actual fertilization of the egg are quite
unknown in Nautilus, and imperfectly in the Dibranchs
and the Pteropoda. Allusion has already been made to
the subject in connexion with the hectocotylized arm. The
mature eggs of Nautilus are unknown, as well as the appear-
ance which they present when deposited. In the Dibranchs
the eggs are always very large ; in some cases the amount
of food-yelk infused into the original egg-cell is so great aa
to give it the size of a large pea. This results in that
mode of development which is only known outside this
class among the Vertebrata ; it is discoblastic. The proto-
plasm of the fertilized egg-cell segregates to one pole of
the egg, and there undergoes cell-division, resulting in the
foi-mation of a disc of cleavage cells (fig. 121, (1)) resem-
bling the cicatricula of the hen's egg, which subsequently
spreads over and invests the whole egg (fig. 121, (2)).- For
details of this process we must refer the reader to other
works (45, 46) ; but it may here be noted that in addition to
the layer of cleavage cells, v;hich consists of more than one
stratum of cells in the future embrj'onic area as opposed
to the yelk-sac area, additional cells are formed in the
mass of residual yelk apparently by an independent process
of segregation, each cell having a separate origin, whence
they are termed "autoplasts." The autoplasts eventually
form a layer of fusiform c^s (fig. 121, (7), h; fig. 122, m;
and fig. 123, ps), — the "yelk-membrane" which everywhere
rests upon and encloses the residual yelk. The cleavage
cells form a single layer on the yelk-sac area and two layers
on the embryonic area, an outer layer one cell deep (fig. 122,
ep), and an inner — tiie middle layer of t!ie three — wluch
is often thick and many cells deep (fig. 122, m). There is
great difficulty here in identifying the layers with the three
typical layers of other animal embryos, except in regard
to the outermost, which corresponds with the epiblast of
Vertebrates in many respects. The middle layer, howe\'er,
gives rise to the nerve-ganglia as well as to the muscles,
coelom, and skeleto-trophic tissues, and to the mid-portion
of the alimentary canal with its hepatic diverticula, the
liver (see fig. 121, (7) and explanation, where the origin of
the mid-gut as a vesicle r is seen). It is clearly, therefore,
something more than the mesoblast of the Vertebrate,
giving rise, as it does, to important organs formed both by
epiblast and hypoblast in other animals. Lastly, the yelk-
meifibrane, though corresponding to the Vertebrate hypo-
blast in position and structure, furnishes no part of the
alimentary tract, but di.sappears when the yelk is com-
pletely absorbed. In fact, the developmental phenomena
in Sepia, Loligo, and Octopus are profoundly perturbed by
>the excessive ijroportion of food-yelk. Balfour has shown
OEFBJXOPODA.]
that in the chick the orifice o£ closure of the overspreading
blastoderm does not represent the whole of the blastopore,
MOLLUSCA
683
a structure corresponding to the primitive streak of the
chick, and lying near the klastic pole, will be found in
Sepia and Loligo, and the strange vesicular origin of the
mid-gut will be traced to and explained by it.
Leaving this difficult question of the cell-layers of the
embryo, we would draw the reader's attention to the series
of sketches representing the semi-transparent embryo of
Loligo, drawn in fig. 121. When the cleavage cells have
nearly enclosed the yelk, the upper or embryonic area
shows the rudiments of the centro-dorsal mantle-sac or
pen-sac, the mouth, the paired optic pits, and the paired
Via. Wl.— Development of Loligo. 0) View of the cleaTuge of tic egg during
■the first formation of embryonic cells. (2) lateral view of the egg at a little
later stage, a, limit to which the layer of cleavage.oeUa has spread over the
egg; t>,portion of the egg(sb3ded)a8yet tincovered byclea^'age-cells; a;>, the
aotoplaata ; kp, cleavage-pole where £f5t cells wen formed. (3) Later stage,
the hmjt a now extended so as to Jeave but little of the egg'aur&ce lb) onen-
dosed. Thoeyes(dX mouthC^X and mantle-sac(u)haveappefind. f4) Later
ftage, anterior sorface, the embryo is becoming nipped off from the yelk
•ac (JX (5) View of an embryo similar to (3) from the cleavagc-pcle or
eentro-dorsal ar^a. (6) Later stage, posterior sorface. (7) Section in a
median dorso-ventral and autero-posterior plane of an embryo of the same
■ge as (4). (8) View of the anterior face of an older embrytx (B> View cf the
posterior face of an embryo of the same age as (8X Letters in (3) to (9) : — a,
lateral fins of the mantle ; h, mantle-skirt ; c, supra-ocular invagination to
form.tbe " white body " ; d, the eye ; e, the month ; /i, », 5, *, 8, the five paired
processes of the fore-foot ; g, rhythmically contractile area of the yeUt-sac,
which is itself a hemia-like protnision of the median portion of the fore-foot
(see fig. 72*'); h, dotted line showing internal area occupied by yelk (food-
material of the egg) ; k, first rudiment of the mid-foot (paired ridges which
onite to form the siphon or fUnnel) ; I, sac of the radula or lingual ribbon ;
m, stomach ; n, rudiments of the gills (paired ctenidia) ; o, the otocysts. — a
pair of invaginations of the surface of the raid-foot ; J>, the optic ganglion ;
a, the distal portion of the ridges which fonn the siphon or mid-foot, k being
the basal portion of the same structure; r, thevesicle-liice rudimentofthe in-
testine formed independently of the parts connected with the mouth, s, ?:, m,
«nd without Invagination ; s, rudiment of the salivary glands ; t in (7X the
Bhell-eac at an earlier stage open (see Hg. 13SX now closed up; u, the open
<hell-sac formed by an uprising ring-like growth of the centro-dorsal area ;
V in (5), the mantle-skirt commencing to be raised up around the area of the
diell-sac. In (7) mes points to the middle cell-layer of the embryo, ep to the
outer layer, and h to the deep layer of fusiform cells which separates every-
where the embryo flrom the yelk or food-material lying within it, (Original.)
h«it that this is in part to be sought in the vridely-separated
primitive streak. The present writer has little doubt that
Fin. 122.— Section through the still open shell-sac occupying the centro-dorsal
area of an embryo of L/>liso ; the position is inverted as compared with fig.
121 (3) and (7). ep, outer ccll-hiyer ; <,t, middle cell-layer ; m'. deep cell-
layer of fusiform coUs ; y, the granular yelk or food-material of the egg ;
ths, the still open sUeU-sac (Proui Lankcster.)
Otic pits (fij. 121, (3), (5)). The eye-pits close -up (fig.
119), the orifice of the mantle-sac narrows, and its margin
becomes raised and freely produced as mantle-skirt ;
at the same time an hour-glass-like pinching in of the
whole embryo commences, separating the embryo proper
from the so-called yelk-sac (fig. 121, (4)). Around the
" waist " of constriction, pair by pair, ten lobes arise (fig.
121, (8) ), — the arms of the fore-foot. It now becomes
obviou.3 that the yelk-sac is but the median surface of the
fore-foot bulged out inordinately by food-yelk, just a3 the
hind region of the foot is in the embryo slug (see fig. 72**,
and ex-planation). Just as in the slug, this dilated y(jjk-
holding foot is rhythmically contractile, and pulsates
steadily over the area ff in fig. 121, (■!). At this stage,
and long subsequently, the mouth of the young Cephalopod
is in no way surrounded by the fore-foot, but lies ^vell
above its nascent lobes (e in fig. 121). Subsequently it
sinlcs, as it were, between the right and left most anterior
pair of the series, which grow towards one another and
fuse above it, and leave no trace of their original position
and relations. Fig. 121, (6) gives a view of the postero-
dorsal surface of an embryo, in which the important fact
is seen of the formation of the funnel or siphon by the
union of two pieces (q), which grow up each independently,
one right and one left, like the sides of the siphon of
Nautilus or the sv/imming lobes of a Pteropod, and subse-
quently come together, as shown in (9), where the same
letter 9 indicate.s the same part. The explanations of figs.
121 and 123 are given very full and here, therefore, we
shall only allude to two additional points. A curious mass
of tissue of unknown significance occurs in the orbit of
Dibranchs, known as the white body (iv in fig. 120). A
strongly-marked invagination just above the orbit is a very
prominent feativre in the embryo of Loligo, Sepia, and
Octopus, and appears to give rise to this so-called white
body. This invaginated portion of the outer cell-layer is
seen in fig. 121, (8) and (9), lettered c; in fig. 123, A and
B, it is lettered vjb.
Lastly, in fig. 123, A, the origin of the optic neiY;:-
ganglion r^ from the cells of the middle layer shouli'. b?
especially noticed. In some other Molluscs the ner'O-
ganglia have been definitely traced to the outer cell-layer,
B84
MOLLUSCA
[LiilELLMEANCULi.
Tpl'.ilst in some Gastropods, according to Bobretzky, tliey
ori!:^nate, as here sliown, for Loligo.
The egg-coverings of the Dibranchiate are very complete.
Argonauta and Octopus deposit each egg in a firm oval
ca. [', thin and transparent, which has a long stalli by
-which (in Octopus) tlie egg is fixed in company with two
or three hundred others to some foreign object. Sepia
encloses each egg in a thick envelope of many layers
resembling india-rubber. Loligo encloses many rows of
eggs in a copious tough jelly, and affixes a dozen or twenty
such egg-strings to one spot. Sepia and Loligo desert
their eggs when laid. The female Octopus most jealously
Tlo. 123.— Right and left sections through erat yos of Loligo. A. Same stage
as flg. 121 (4). B. Same stage as lig. 121 (S) ; only the left side of the sections
is drawn, and the food-material wliich occupies the space internal to the
memhrane ym is omitted, at, rccluni ; is, inl;-sac ; cp, outer cell-layer ; mej,
\nicMle cell-layer; i/ni, deep cell-layer of fusiform cel]^ (yellt-memljrane) ; ng,
optic neiTCganglion ; ot, otocyst ; «'6, the " white body " of the adult oc Jar
capsule forming as an invagination of tlie outer cell-layer ; mtf, mantle-skirt ;
g, gill ; ps, pen--iac or shell-sac, now closed ; dg, dorsal groove ; poc, primitive
optic vesicle, now closed (see llg. 110); /, lens ; r, retina ; soc, second or anterior
optic chamber still open ; if, iridean foils. C. The primitive invagination to
form one of the otocysts, as seen in 8g. 121 (5) and (G). (.\fter Lanltcster.)
guards them, building a nest of stones and incubating.
Argonauta carries hers with her in a special brood-holding
shell.
The development of the Pteropoda, so far as is known,
presents no points of contact with that of the Siphonopoda
rather than with that of the Gastropoda, owing to the fact
that in them the egg has not an excess of food-yelk. Con-
sequently, we find tyjiical trochosphere and veliger larva;
among the Thecosomata (fig. 8, C, and fig. 81), whilst the
isolated observation of Gegenbaur has made known very
remarkable larvje referable to the Gymnosomata, and with
little doubt to Pneumodermon (fig. 8-1). The former set of
larvje are sufficient to dom jlish once for all the view which
has been entertained by some zoologists, viz., that the velar
disc of the veliger larva is the same thing as the ptero-
podial lobes of the mid-foot of Pteropoda. The latter
larvse are of importance in showing that, as in embryo
Siphonopods r,o in embryo Pteropoda, the sucker-bearing
lobes of the fore-foot arc truly podial structures, and only
embrace the head and surround the mouth as the result of
late embryonic growth.
Beanch B.—LIFOCEPITALA.
Characters. — Mollusca with the head region undeveloped.
No cephalic eyes are present ; the buccal cavity is devoid
of biting, rasping, or prehensile organs. The animal b
sessile, or endowed with very feeble locomotive powers.
The Lipocephala comprise but one class, the Lamelli-
branchia, also known as Elatobranchia and Conchifera.
Class LAMELLIBEANOHTA
Characters. — Lipocephala in which the archaic BILA-
TERAi, SYMMETEY of the MoUusca is usually fully retained,
and raised to a dominant feature of the organization by the
Literal compression of the body and the development of the
shell as two bilaterally symmetrical plates or valves cover-
ing each one side of tlie animal. The foot is commonly a
simple cylindrical or ploughshare-shaped organ, used for
boring in sand and mud, and more rarely presents a crawl-
ing disc similar to that of Gastropoda ; in some forms it is
aborted. The paired CTENiDLi are very greatly developed
right and left of the elongated body, and form the most
prominent organ of the group. Their function is chiefly
not respiratory but nutritive, since it is by the currents
produced by their ciliated surface that food-particles are
brought to the feebly-developed mouth and buccal cavity.
The LameUibranchia present as a whole a somewhat
uniform structure, so that, although they are vei7 numerous,
it is not possible to divide them into well-marked sub-classes
or sections, and orders. The chief points in which they
vary are — (I) in the structure of the ctenidia or branchial
plates ; (2) in the presence of one or of two chief muscles,
the fibres of which run across the animal's body from one
valve of the shell to the other (adductors) ; (3) in the greater
or less elaboration of the posterior portion of the mantle-
skirt so as to form a pair of tubes, by one of which water
is introduced into the sub-pallial chamber, whilst by the
other it is espeUed ; (4) iu the perfect or deficient symmetry
of the two valves of the shell and the connected soft parts,
as compared vnih one another ; (5) in the development of
the foot as a disc-like crawling organ (Area, Nucula, Pectun-
culus, Trigonia, Lepton, Galeomma), as a simple plough-
like or tongue-shaped organ (Unionacea, &c.), as a re-curved
saltatory organ (Cardium, &c.), as a long burrowing cylin-
der (Solenacea, &c.), or its partial (Mytilacea) or even com-
plete abortion (Ostracea).
The essential MoUuscan organs are, with these excep-
tions, uniformly well developed. The m.u«-tle-skiet is
always long, and hides the rest of the animal from view, its
dependent margins meeting in the middle line below the
ventral surface when the animal is retracted ; it is, as it
w'ere, slit in the median lino before and behind so as to
form two flaps, a right and a left ; on these the right and
the left calcareous valves of the shell are borne respectively,
connected by an uncalcified part of the shell called the
ligament. In many embryo LameUibranchs a centro-dorsal
PRIMITIVE snELl/-G7-,AND Or foUicle has been detected (figs.
8 and 151). The mouth lies in the median line anteriorly,
the .iUnjs in the median line posteriorly.
Both CTEisriDiA right and left are invariably present, the
axis of each taking origin from the side of the body as in
the schematic arehi-MolIusc (see fig. 1 and fig. 131). A
pair of SErHKiDfA opening right and left, rather far forward
on the sides of the body, are always present. Each opens
by its internal extremity into the pericardium. A pair of
GENITAL APESTrrRE-s, connected by genital ducts with the
paired gonads, are found right and left near the nephridial
pores, except in a few cases where the genital duct joins
that of the nephridium (Spondylus). The sexes are often,
but not always, distinct. No accessoiy glands or copulatoty
organs are ever present in LameUibranchs. The ctenidia
often act as brood-pouches.
A dorsal contractile nEir.T, with symmetrical right and
left auricles (fig. 1 43, A) receiving aerated blood from the
ctenidia and mantle-skirt, is present, being unequally do-
T,AMFT-T.rRB.AKfTTrrA^1
MOl^LUSCA
686
veloped only in those few forma which are ineqvuvalve.
The typical PEKicAKDrtTM is well developed. It appears,
as in other MoUusca, not to be a blood-space although
developed from the coelom, and it conununicates with the
exterior by the pair of nephridia. As in Cephalopoda (and
possibly other MoUusca) water can be introduced through
the -nephridia into this space. The at.tmentaby canal
keeps very nearly to the median vertical plane whilst ex-
hibiting a number of flexures and loopings in this plane.
A pair of large glandular outgrowths, the so-called " liver "
or great digestive gland, exists as in other MoUuscs. A
pair of pedal otocysts, and a pair of osphkadia at the
base of the gills, appear to be always present. A typical
NEEVOUS SYSTEM is present (fig. 144), consisting of a
cerebro-pleuro-visceral ganglion-pair, united by connectives
to a pedal ganglion-pair and an osphradial gang!ion-pair
(parieto-splanchnic).
A special CKCum connected with the pharynx is some-
times found, containing a tough flexible cylinder of trans-
parent cartilaginous appearance and unknown significance,
called the "crystalline style" (Mactra), which possibly
represents the radular sac of Glossophora. In manyLamelli-
branchs a gland is found on the hinder surface of the foot
in the mid line, which secretes a substance which sets into
the form of threads — the so-called " byssus " — by means of
which the animal can fix itself. Sometimes this gland is
found in the young and not in the adult (Anodon, Unio,
Cyclas). In some Lamellibranchs (Pecten, Spondylus,
Pholas, Mactra, Tellina, Pectunculus, Galeomma, &c.),
. although cephalic eyes are always absent, special eyes
are developed on the free margin of the mantle-skirt,
apparently by the modification of tentacles which are
commonly found there (fig. 145). The existence of pores
in the foot and elsewhere in Lamellibranchia by which liquid
can pass into and out of the vascular system, although
asserted as in the case of other MoUusca, appears to be
improbable. It has yet to be shown by satisfactory micro-
scopic csctions that the supposed pores are anything but
epidermal glands.
The Lamellibranchia live chiefly in the sea, some in
fresh waters. A very few have the power of swimming by
opening and shutting the valves of the shell (Pecten, Lima) ;
most can slowly crawl or rapidly burrow; others are, when
adult, permanently fixed to stones or rocks either by the
shell or the byssus. In development some Lamellibranchia
pass through a free-swimming ti-ochosphere stage with prae-
oral ciliated band ; other fresh-water forms which carry the
young in brood-pouches formed by the ctenidia have sup-
pressed tliis larval phase.
The following classification and enumeration of genera
are based primarily upon the characters of the adductor
muscles. The Heteromya and Monomya must be conceived
of as derived from forms resembling such Gastropodous
Isomya as Nucula and Trigonia, which undoubtedly are
the nearest living representatives of the ancestral Lipo-
cephala, and bring us nearest to the other branch of the
MoUusca, the Glossophora.
Ordor 1. — laomya.'
Character. — Anterior and posterior adductor muscles of approxi-
mately equal size.
Sub-order 1. — InlegripalUa.
Cftarodwa.— Marginal attachment of the mantle to the shell not
inflected to form a sinua ; siphons not developed in some, present
in most.
Family 1. — Arcacea.
Genera : Area., L. (fig. 132) ; Cucullasa, Lam. ; Pectunculus, Lam. ;
Limopsis, Sassl; Nucula, Lam. (fig. 134) ; laoarea, Munster ;
Leda, Schu. ; Foldia, MoIL ; Solenclla, Sowerby, &c.
Family 2. — Trigoniacea.
Genera : Trigonia, Brug. ; Axinua, Sow. ; Lyrodeama, Conrad.
Family 3. — Unionaeea.
Genera: Vnio, Eetz. ; Castalia, Lam. ; Anodon, Cuv. (figs. 124
&C.) ; Iridina, Lam. ; Mycetopui, d'Orb., fcc.
Family i. — tueinaeea.
Genera : Lucina, Brug. ; CorHs, Cuv. ; Diplodmla, Brown ;
Kellia, Turton ; Mmtamta, Turton ; Lepton, Turton ; Oale-
cnnma, Turton ; Astarte, Sow. ; Crassatdla, Lam. j Cardinia,
Ag. ; Cardita, Brug., &c
Family 5. — Cyprinaeea.
Genera : Tridacna, Da C.'; Chama, L. ; Dimya, Ron. ; Diceras,
Lk. ; lioeardia, Lam. ; Bippopodium, Sow. ; Cardium, L. ;
Corbieula, Meg. ; Cyrena, Lk. ; Cyclas, Brug. (fig. 146) ; Piind-
ium, Pfr. (figs. 148-153) ; Cyprina, Lam., &c.
Sab-order 2. — Sinupallia.
CSorscfers.— Marginal attachment of the mantle to the shell in-
flected so as to form a sinus into which the pallial aiphons can l»
withdrawn ; siphons always present, and large.
Family 6. — Veriercuxa.
Genera : Cypricardia, Lam. ; Tapes, Megl. ; Cyclina, Desh. ■,
Cytherea, Lam. (figs. 125, &c.) ; Chime, Megl. ; Vemia, L. ;
Liidnopsis, F. H. ; Sanguinolaria, Lam. ; Psammobia, Lam.
(fig. 130) ; . Tellina, L. ; Vonax, L. ; Scrobicularia, Schu. ;
Cumingia, Sow. ; Bangia, Dsml ; Maelra, L. (fig. 140) ; Trigo-
nella, Da C. ; Vaganclla, Gr. ; Lutraria, Lam.
Family 7. — Myacea.
Genera : ilycchama, Stb. ; Chamosirea, Eois ; Pandora, Sol. ;
Thracia, Leach ; Thetis, Sow. ; Pholadomya, Sow. ; Corhula,
Brug. ; Mya, Lam. ; Saxicava, Fleur ; Panopma, Ad. ; Olyei-
meris, Lam. ; Siliqua, Mhlf., &c. ; Solen, L.
Family 8. — Pfioladacea.
Genera : Clavagella, Lam. ; AspergiUum, Lam. (figs. 128, 129) ;
Humphrajia, Gr. ; Pholas, L. ; Pholadidea, Turt. ; Teredo, L. ;
Teredina, .Lam. ; Furcella, Oken, &c.
Order 2. — Heteromya.
Charaeters. — Anterior adductor (pallial adductor) much smaller
than the posterior adductor (pedal adductor) ; siphons rarely present
Family 1. — Mytilacea.
Genera : Mytilus, L. (fig. 133); Modiola, Lam.; Crenella, Brown ;
Lithodomus, Cuv. ; Dreissena, Ben. (fig. 136) ; Modiolarea,
Gr., &c.
Family 2. — Mulleriacea.
Genera : Aetheria, Lam. ; Mulleria, Vir.
Order 3. — Monomya.
Characters — Anterior adductor absent in the adult
never developed.
Family 1. — Anculacea,
Genera : Cardiola, Brdp. ; Avicula, Kl. ; Malleus, Lam. ; /tw-
ceramtu. Sow. ; Crenatula, Lam. ; Perna, Brug., &c.
Family 2. — Ostracea.
Genera: Osirea, L. (fig. 6); Anmnia, L. ; Spondylus, L. ; Plicatula,
Lam. ; Vulsella, Lam. ; Lima, Brug. ; Pecten, L. ; Siuniles,
Dfr., &c.
Further Remarhs on the Lamellibranchia. — The Lamelli-
branchia are the only members of the Lipocephalous branch
of MoUusca existing at the present day; and we must
suppose that, whilst on the one hand the earliest Glosso-
phorous forms were developing from the archi-Mollusca by
the elaboration of the buccal apparatus, the bivalvcd sessile
Lamellibranchs were developing in another direction from
univalve cephalophorous ancestors. The large bilobed
mantle-flap witb its pair of shells covering in the whole
animal, the current-producing largely-expanded ctenidia,
and the reduced cephalic region ars characters which go
hand in hand, and were simultaneously acquired, each being
related to the development of the others. Unless the
" crystalline style " of Lamellibranchs is to be considered
as the rudiment of the " radular sac " of Glossophora, as
suggested by Balfour, there is no indication whatever that
the ancestors of the LameUibranchia had acquired a repre-
sentative of the buccal apparatus— so highly developed in
Glossophora— before diverging from the archi-MoUusca ;
that is to say, the common ancestors of the two great
branches of MoUusca presented the distinctive character
of neither branch — they had not an aborted cephalic region,
and they had not a lingual ribbon.
As an example of the organization of a Lamellibranch,
we shaU review the structure of the Common Pond-Mussel
{Anodonta cygnea), comparing its structure with those of
686
MOLLUSCA
[lamzj-ubeabchia;
other Lamellibraucliia. The Swan ifussel has superSciaJiy
a_ perfectly-developed bilateral symmetry. The left side, of
the animal is seen as when removed from its shell in fig.
124 (1). The valves of the shell have been removed by
severing their adhesions to the muscular areje h, i, k, I, m, u.
(1) Z f ^ "i. ? ? f 0 „;j
?I0. 124. — DiJi^T-ims of the external form and anatomy of Anodonia cyynca, the
Pond-Ma-ssei': in all the figures the animal is seen from the left aide, the
centixMlorsai region appermost, as in the drawings of fig. 75, which compare,
(i) Animal removed from its shell, a probe g passed into the sab-pallial
chamber through the excurrent Biphonal notch. (2) View from the ventral
FOTliice of an Anodoo with its foot expanded and issuing from between the
::.".Ding shells. (3) The left mantle. flap reflected upwards so es to expose the
sides of the body. (4) Diagrammatic section of AnoJon to show the course of
the alimentary canal. (5) The two gill.plates of the left side reflected upwards
so as to expose the fissure between foot and gill where the probe g passes.
(6) Diagram to show the positions of the ncrve.ganglia, heart, and nephridia.
Letters in all the figures as follows '.-~-a^ centro-dorsal area ; b, m.argin of
the left mantle-flap ; c, margin of the right mantle- flap ; d, excurrent siphocal
notch of the mantle margin : e, incurrent siphonal notch of the mantle
fix)t ; k, proti-actor muscle of the foot ; I, posterior (pedal) adductor muscle
of the shells ; m, posterior retractor muscle of the foot ^n, anterior labial
tentacle ; o, posterior labial tentacle ; p, base-line of origin of the reflected
mantle-flap from the side of the body ; 9, left external gill-plate ; r, left In-
^-.-nal gill-plate ; iv. Inner lamella of the right muer gill-plate ; rf?, right outer
gill-plate : *, line of concrescence of the outer lamella of the left outer gill-
plate with the left mantle-flap ; t, pallial tentacles ; v, the thickened mtis-
cular pallial margin which adheres to the shell and forms the pallial line of
the left side ; v, that of the- right aide ; w, the mouth ; r, aperture of the left
organ of Bojanus (nepliridium) exposed by cutting the attachment of the
inner lamella of the inner gill-plate ; y, aperture of the genital duct ; «, fissure
between the free edge of the inner lamella of the inner gill-plate and the side
of the foot, through which the probe g passes into ttie upper division of the
aub-pallial space ; oa, line of concrescence of the iimcr lamella of the right
inner giU.pl.ate with the inner lamella of the lef^ iunrr gill-plate ; ri, ac, ad,
three pit-like depressions in the median lino of tlie lont supposed by some
writ>u^ to he pores admitting water into the vascular system ; oe, left shell
valve ; i^f, space occupied by liver ; ag, spac" occitoicii by i^.mad ; ah, muscular
substance of the foot : ai, duct of the liver on ifie w.iU of the stomach ; afc»
stomach ; at, rectum traversing the ventricle of the licavi ; 07.1, pericai?iinm ;
an, glandular portion of the left nephridium ; ap, ventricle of Ihe heart ; uq,
aperture by which the left auricle joined the ventricle ; or. non-glandular por-
tion of the left nephridium ; as, anns ; at, pore leading fVom the pericardium into
the glandular sac of the left nephridium ; aii, pore leadin,'* from the glandular
into the noU'glandular portion of the left nephridium ; av, internal pore lead-
ing from the non-glandular portion of the left nephridium to the external
pore r; aie, left cerobro-pleuro-viaceral ganglion: ax, left peditl ganglion;
ay, left otocyst ; (ir, left olfactory ganglion {narieln-snlanehnic) ; ^^ floor of
the pericardi-m separating that space from tne non-ylandulnr portion of tie
nephridia.
The free edge of the left half of the mantle-skirt b is repre-
sented as a little contracted in order to show the exactly simi-
lar free edge of the right half of the raantle-.skirt c These
edges are not attached to, nUuough they touch, one auother;
each flap (nKht or left) can be freely thrown back in the way
which has been carried out in fig. 1 24, (3) for that of the
left side. This is not always the case with Lamellibranchs ;
there is in the group a tendency for the corresponding
edges of the mantle-idrt to fuse together by concrescence,
and so to form a more or less completely closed bag, as in
the Scaphopoda (Dentalium). In this way the notches
d, e of the hinder part of the mantle-skirt of Anodon are in
the Siphonate forms converted into two separate holes, the
edges of the mantle being elsewhere fused together along
this hipder margin. Further than this, the part of the
mantle-skirt bounding the two holes is frequently drawn out
so as to form a pair of tubes which project from the 8hell(figs.
130, 141). In such Lamellibranchs as the oysters, scallops,
and many others which have the edges of the mantle-slort
quite free, there are numerous tentacles upon those edges.
In -Ajiodon these pallial tentacles are confined to a small area
surrounding the inferior siphonal notch (fig. 124, (3), !l).
The centre-dorsal point a of the animal of Anodonta
(fig. 124, (1)) is called the umbonal area ; the great anterior
muscular surface h is that of the anterior adductor muscle,
the posterior similar surface t is that of the posterior
adductor muscle ; the long line of attachment « is the
simple " pallial muscle," — a thickened ridge which is seen
to pun parallel to the margin of the mantle-skirt in this
Lamellibranch. In some of the Siphonate Isomya, which
are hence termed " Sinupallia," the pallial muscle is not
simple but deeply incurved at the posterior region so as to
allow of the large pallial siphons being retracted within the
shell or expanded at will (fig. 127, and figs. 140, 141).
It is the approximate equality
in the si^e of the anterior and
posterior adductor muscles which
has led to the name Isoyma for
the group to which -Anodon be-
longs. The hinder adductor
muscle may be considered as re-
presenting morphologically the I
transvei^e fibres of the root of
the foot of Nautilus by which it '
adheres to its shell (fig. 91, i), the
annular muscular area of Patella
(fig. 2 7,c), and the columella muscle
of the Gastropods generally. It
is always large in Lamellibranchs,
but the anterior adductor may
be very small (Heteromya), or^'°;}2
, ^ ■" ,, ..^ ,,, ■' ' ^ of the shell of Cythcrea (one of
absent altogether (Monomya). the sinnpaiiiate isomyai tmt
The anterior adductor muscle is ""= ''"'^ "P««-
in front of the mouth and alimentary tract altogether,
and must be regarded as a special and peculiar deve-
lopment of the median anterior part of the mantle- Sap
liganuDt
T of the two v«lvc3
'^rnlorinicTioT ho^*
Fio. 120.— Right valve of the aamc shell from the outer face.
in Heteromya and Isomya. Amongst those Lamelli-
branchs which have only a posterior adductor (Monomya),
it is remarkable that the oyster has been found (by
Huxley) to possesi, when the young shells and muscle i
first develop, a well-marked anterior adductor as \/ell as a
posterior one. Accordingly there is ground for supposing .
l.AnntT.T.rHBiN-ran J
AJ O L L U a C A
687
that the Monomya have been developed from Isomya-
like ancestors, and have lost by atrophy their anterior
adductor. The single adductor zniLscle of the Monomya
is separated by a
difference of fibre
into two portions,
but neitherof these
can be regarded as
possibly represent
ing the anterior
adductor of the
other Lamelli-
branchs. One of
these portions is
more ligamentous,
and serves to keep
the two shells con-
stantly attached to
one another, whilst Fio. 127.— Left ralve of the
the more fleshy por-
tion serves to close the shell rapidly when it has been gaping.
In removing the valves of the shell from an Anodon, it
is necessary not only to cut through the muscular attach-
ments of the body-wall to the shell but to sever abo a
strong elastic ligament, or spring resembling india-rubber,
joining the two shells about the umbonal area. The shell
«f Anodon does not present these parts in the most strongly
marked condition, and accordingly our figures (figs. 125,
126, 127) represent the valves of the Sinupalliate genus
Cytherea. The corresponding parts are recognizable in
Anodon. Referring to the figures (125, 126) for an ex-
planation of terms applicable to the parts of the valve and
the markings on its inner surface — corresponding to the
muscular area which we have already noted on the surface
of the animal's body — we must specially note here the posi-
tion of that denticulated thickening of the dorsal margin
of the valve which is called the hinge (fig. 127). By this
liinge one valve is closely fitted to the other. Below this
binge each shell becomes concave, above it each shell rises a
little to form the umbo, and it is into this ridge-like upgrowth
of each valve that the elastic ligament or spring is fixed (fig.
127). As shown in the diagram (fig.
127*) representing a transsverse sec-
tion of the tvi'o valves of a Lamelli-
branch, the two shells form a double
lever, of which the toothed- hinged is
the fulcrum. The adductor muscles
placed in the concavity of the shells a-
act upon the long arms of the lever
at a mechanical advantage ; their con-
traction keeps the shells shut, and
stretches the ligament or spring A.
On the other hand, the ligament h
acts upon the short arm formed b}
the umbonal ridge of the shells; when-
ever the adductors relax, the elastic
substance of the ligament contracts,
and the shells gape. It is on this
account that the valves of a dead La- '",
mellibranch always gape ; the elastic «'
ligament is no longer counteracted by
the effort of the adductors. The state
of closure of the valves of the shell is
not, therefore, one of rest ; when it is
at rest — that is, when there is no
muscular effort — the valves of a Lamellibrancb are slightly
gaping, and are closed by the action of the adductors when
the animal is disturbed. The ligament is simple in Anodon ;
in many Lamellibranchs it is separated into two layers, an
outer and an inner (thicker and denser). That the condition
tion of a Laiiiellibrancli'd
nliclls, ligaiiicnt, and ail-
ductor muscle, a, b, riglit
and led valves of the
shell ; c, d, the umlxines
or short ai ms of the'
(,/ the long
-.J. the hinge: ft, th
leTvei
i ol^tl
ligaiiie
, the adductor
of gapug of the shell-valvea is essen'tial to the life of the
Lamellibrancb appears from the fact that food to nourish
it, water to aerate its blood, and spermatozoa to fertilise
its eggs, are all introduced into this gaping chamber by
currents of water, whicli are set going by the highly-
developed ctenidia. The current of water enters into the
Bub-pallial space at the spot marked e in fig. 124, (1),
and, after passing as far forward as the mouth w in fig. 124,
(5), takes an outward course and leaves the sub-pallial
space by the upper notch d. These notches are knovra
in Anodon as the afferent and efferent siphonal notches
respectively, and correspond to the long tube-like afferent
interior and ctfertnt superior "siphons" formed by the
mantle in many other Lamellibranchs (fig. 130).
AVliilst the valves of the shell are equal in Anodon we
find in many Lamellibrancrfs (Ostraea, Chama, Corbula, &c.)
one valve larger, and the other smaller and sometimes flat,
whilst the larger shell may be fixed to rock or to stones
(Ostrsea, ic). A further variation consists in the develop-
ment of additional shelly plates upon the dorsal line be-
tween the two large valves (Pholadida;). In Pholas dadylvs
we find a pair of umbonal plates, a dors-nmbonal plate and
a dorsal plate. It is to be remembered that the whole of the
cuticular hard product produced on the dorsal surface and
on the mantle-flaps is to be regarded as the "shell," of
which a median band-like area, the ligament, usually remains
uncalcified, so as to result in the production of two valves
united by the elastic ligament. But the shelly substance
does not always in boring forms adhere to this form after
its first growth. In Aspergillum the whole of the tubular
mantle area secretes a continuous shelly
tube, although in the young condition two
valves were present. These are seen (fig.
129) set in the firm substance of the adult
tubular shell, which has even replaced the
ligament, so that the tube is complete. In
Teredo a similar tube is formed as the animal
elongates (boring in wood), the original ahell-
valves not adhering to it but remaining mov-
able and provided with a special muscular
apparatus in place of a ligament.
Let us now examine the organs which lie
beneath the mantle-skirt of Anodon, and are
bathed by the curr«nt of water which cir-
Fig. 129.
1 (from Owen).
)i to 8ho\T the original valves
bular fonu (from Owen).
Fig. 128.
Fio. 12s.— Shell t>t A^ptrgVXum vPQiT.ifrr
Fio. 129.— Shell ot AsixrgiUttm fojiuyinnii I,
embedded in a continuous calciticatiou of t
culates through it. This can be done by lifting up and
throwing back the left half of the mantle-skirt as is re-
presented in fig. 124, (3). We thus expose the plough-
like foot (/), the two left labial tentacles, and the two
left gill-plates or left ctenidium. In fig. 124, (5), one of
the labial tentacles « is also thrown back so as to diow
688
MOLLUSCA
[lauellibkajichia.
the mouth if, and the two left gill-plates are reflected
so as to show the giU-plates of the right side {rr, rq) pro-
jecting behind the foot, the inner or median plate of each
side being united by concrescence to its fellow of the
opposite side along a continuous line {aa). The left inner
gill-plate is also snipped so as to show the subjacent orifices
of the left nephridium x, and of the genital gland (testis or
ovary) y. The foot thus exposed in Anodou is a simple
muscular tongue-like organ. It can be protruded between
the flaps of the mantle (fig. 124, (1), (2)) so as to issue
from the shell, and by its action the Anodon can slowly
crawl, or burrow in soft mud or sand. It has been sup-
posed that water is taken into the blood-vessels of the
Anodon through pores in the foot, and in spite of opposi-
tion this view is still maintained (Griesbach, 47). In fig.
124, (2) the letters ab, ac, ad, point to three pit-like depres-
sions, supposed by Griesbach to be pores leading into the
blood-system. According to Carriere (48) these pits are
nothing but irregularities of the surface ; in some cases
they are the entrances to ramified glands. Other Lamelli-
branchs may have a larger foot relatively than has Anodon.
In Area it has a sole-like surface. In Area too and many
others it carries a byssus-forming gland and a byssus-
cementing gland. In the Cockles, in Cardium, and in
Trigonia, it is capable of a sudden stroke, which causes
the animal to jump when out of the water, in the latter
"mm
Tia 130. — P<ammobUi floridi
genus to a height of four feet. In Mytilus the foot is
reduced to little more than a tubercle carrying the aper-
tures of these glaa^ls. In the Oyster it is absent alto-
gether.
The labial tentacles of Anodon (n, o in fig. 124, (3), (5) )
are highly vascular
flat processes richly
supplied with nerves.
The left anterior ten-
tacle (seen in the
figure) is joined at
its base in front of
the mouth (ic) to the
right anterior ten-
tacle, and similarly
the left (o) and right
posterior tentacles
are joined behind the
mouth. Those of _ ., _, , . , »^ , „ . . ,
Area (l, K m ng. l-i-i) the animal ot Anodonta cygnica, from which the
show tliiii rpl.ation to "anHesklrt, the labial ti-ntacles, and the gill-
8U0W lUlS reiauon w (lament, have Ken entirely removed so as to
the mouth (a). These sfiow the relations of the axis of the giU-plmiies
/ . or ctenidia g, k. a, ccntro-dorsal area ; ft, ante-
organs are CCaractei-- rior adductor muscle ; c, posterior adductor
istic of fll Lamelli- tJU8cIe;d, mouth ;e anus ; /toot ;? a-copor.
tion of the axis of left cteuidium ; A, axis of
ri;:ht ctcnidium; k, portion of the axis of the
left ctcnidium which is fused with the base of
the foot, the two dotted lines indicating the
origins of the trio rows of giU-fllamenta ; ft, line
of origin of the anterior labial tentacle ; n, ne-
phildial onerture; o, gcniul aperti
branchs ; they do not
vary except in size,
being sometimes
drawn out to
streamer-like dimen-
sions. Their appear-
ance and position suggest that they are in some way
related morphologically to the gill-plates, the anterior
labial tsntacle being a contiauatiou of the outer gill-plate.
[ the posterior labial tentacle. (Oii-
and the posterior a continuation of the inner gill-plate.
There is no embryological evidence to support this Sug-
gested connexion, and, as will appear immediately, the
history of the gill -plates in various forms of Lamelli-
branchs does not directly favour it. Yet it is very prob-
able that the labial tentacles and gill -plates are modi-
fications of a double horseshoe -shaped area of ciliated
filamentous processes which existed in ancestral Mollusca
much as in Phoronis and the Polyzoa, and is to be com-
pared vdih the continuous prs- and post-oral ciliated band
of the Echinid larva Pluteus and of Tornaria (49).
The giU-plates have a structure very difi'erent from that
of the labial tentacles, and one which in Anodon is singu-
larly complicated as compared with the condition presented
by these organs in some other Lamellibranchs, and with
what must have been their original condition in the ances-
tors of the whole series of living LameUibranchia. The
phenomenon of " concrescence " which we have already had
to note as -showing itself so importantly in regard to the
free edges of the mantle-skirt and the formation of the
siphons, is what, above all things, has complicated the
structure of the Lamellibranch ctenidium. Our present
knowledge of the interesting series of modifications through
which the Lamellibranch gill-plates have developed to their
most complicated form is due to R. Holman Peck (50)
and to Mitsukuri (51). The MoUuscan ctenidium is typi-
cally, as shown in fig. 2, a plume-like struc-
ture, consisting of a vascular axis, on each
side of which is set a row of numerous la-
melliform or filamentous processes. These
processes are hollow, and receive the venous
blood from, and return it again aerated into,
the hollow axis, in which an aflerent and an
efferent blood-vessel may be differentiated.
In the genus Nucula (fig. 134), one of the
urrent Arcaceas, we have an example of a Lamelli-
branch retaining this plume-Uke form of giU.
In other Arcacese (e.ff., Area and Pectunculus) the lateral
processes which are set on the axis of the ctenidium are not
lameUffi, but are slightly-flattened very long tubes or hol-
low filaments. These fila-
ments are so fine and are
set so closely together
that they appear to form
a continuovis membrane
until examined with a
lens. The microscope
shows that the neighbour-
ing filaments are held to-
gether by patches of cilia,
called " ciliated junc-
tions," which interlock
with one another just as
two brushes may be made
to do. In fig. 133, A a
portion of four filaments
of a ctenidium of the Sea-
Mussel (Mytilus) is repre-
sented, having precisely j
the same structure
those of Area. The fila-
ments of the gill (cteni-
dium) of Mytilus and
Area thus form two
Fio. 1S2.— View from tho ventral (pedal) as-
pect of the animal of ArcaXot:, themantle-
OApond giU-filaroents having been cutaway.
a, mouth ; b, anus ; c, fixe spirally turned
extremity of the giU-axis or ct«nidial axis
of the right side ; d, do. of the left side ;
e, /, anterior portions of these axes fused
by concrescence to the wall of the body ;
<?, anterior adductor muscle ; A, posterior
closely set row^ ■which adductor; i, anterior labial tentacle; k,
J I t ^., *!,« rt,.;« «f posterior labial tentacle . ^ baseline of the
depend from the axis ot f^^^. „,^ ^^^^ „f j^.^ f^[.^ ,^ caUoaity.
the gill like two parallel (Original.)
plates. Further, thcii- structure is profoundly modified by
the curious condition of the free ends of the depending
filaments. These arc actually reflected at a sharp angle—
LAMELLIBRANCBIA.]
M O L L U S C A
689
doubled on tnemseives in fact — and thus fonn an additional
row of filaments (see fig. 1 33, B). Consequently, each primi-
tive filament has a descending and an ascending ramus, and
instead of each row forming a simple plate, the plate is
double, consisting of a descending and an ascending lamella.
As the axis of the ctenidium lies by the side of the body,
and is very frequently connate with the body, as so often
happens in Gastropods also, we find it convenient to speak
of the two plate-like structures formed on each ctenidial
axis aathe outer and the inner gill-plate; each of these is
Tvt. 133. — FiUmisnts of the cteoidinm of MyiilvM edulfx (after HoIidad Peck).
A. Part of four tllaments seen from the outer face in order to show the ciliated
janctiona e^. B. Diagram of the posterior (ace of a single complete filament
with descending ramus and ascending ramus ending In a hook-like process.
fp., ep., the ciliated junctions ; iij., inter-lamellar junction. C. Transverse
section of a filament taken so as to cut neither a ciliated Junction lior an
inter-lamellar junction, /.e., frontal epithelium ; I./.e'., IJ.^'-, the two rows
of latero-frontal epithelial ceils with long cilia ; cti, chitonous tubular lining
of the filament ; inc., blood lacnna traversed by a few processes Qf connective
tisane cells ; b.c, Wood-corpuscle.
composed of two lauKllae, an outer (the reflected) and an
adaxied in the case of the outer gill-plate, and an adaxial and
an inner (the reflected) in the case of the inner gill-plate.
This is the condition seen in Area and Mytilus, the so-
called plates dividing upon the slightest touch into their
constituent filaments, which are but loosely conjoined by
their "ciliated jurctions." Complications follow upon
this in othet ionns. Even in Mytilus and Area. a con-
nexion is here and there formed between the ascending
and descending rami of a filament by hollow extensible
outgrowths called " interlamellar junctions " {ilj in B, fig.
133). Nevertheless the filament is a complete tube formed
of chitonous substance and clothed externally by ciliated
epithelium, internally by endothelium and lacunar tissue —
a form of eonnective tissue — as shown in fig. 133, C.
Now let us suppose, as happens in the genus Dreissena —
a genus not far removed from Mytilus — that the ciliated
inter-filamentar junctions (fig. 136) give place to solid
permanent inter-filamentar junction.^, so that the filaments
are converted, as it were, into a trellis-work. Then let us
suppose that the inter-lamellar junctions which we have
already noted in Mytilus become very numerous, large,
aad irregular ; by them the two trellis-works of filaments
would be united so as to leave only a sponge-like set
of spaces between tiieii-.. Within the trabecule of the
sponge-work blood circulates, and between the trabecule
the T-»t« passes, having entered by the apertures left
in the trellis-work fbrmcd by the united gill-filaments
(fig. 138. A, B). The larger the intra- lamellar spongy
Fio. 134.— structure of the ctenidla of Kucula (after Mltanknri) ; see alaa
fig. 2. A. Section across the axis of a ctenidium with a pair of platea—
fiattened and shortened filaments -attached., i, j, 1^ J are placed on or near
the membrane which attaches the axis of the ctenidium to the side of the
body ; o, b, tree extremities of the plates (filaments) ; d, midline of the
inferior border; e, surface of the plate ; (, its upper border; h, chitonous
lining of the plate ; t, dilated blood-space ; «> fibrous tract ; o, upper bl'iod-
vessel of the axis ; n, lower blood-vessel of the axis ; $, chitonous framework
of the axis ; cp, canal in the same ; A, B, line along which the cross-section
C of the plate is taken. B. Animal of a male UuculeL proximo. Say, as seen
when the left valve of the shell and the left half of the mantle-skirt are re-
moved. a.a., anterior adductor muscle ; r-o., posterior adductor muscle :
r.Tn, visceral mass ; / foot ; p, gill ; I, labial tentacle ; i.o., filamentous
appendage of the labial tentacle ; Ih, hood-like appendage of the labial ten-
tacle ; m, membrane suspending the gill and attached to the body along the
line X, y, z,w, p, posterior end of the gill (ctenidium). C. Section across
one of the gill-plates (A, B, in A) comrarable with fig. 133, C. i.a., outer
border; d.a., axial border: I./., latero-frontal epitheliom ; e, epithelium of
general surface ; r, dilated blood-space-; h, chitonous lining (compare A).
growth becomes, the more do the original gill-filaments
lose the character of blood-holding tubes and tend to
become dense elastic rods for the simple purpose of sup-
porting the spongy ^owth. This is seen both in the
section of Dreissena gill (fig. 136) and La those of Anodon
(fig. 137, A, B, C). In the drawing of Dreissena the
individual filaments/, /, / are cut across in one lamella at
the horizon of an inter-filamentar junction, in the other
(lower in the figure) at a point where they are free. " The
chitonous substance ch is observed to be greatly thick'Pned
as compared with, what it is in fig. 133, C, tending in
fact to obliterate altogether the lumen of the filament.
And in Anodon (fig. 137, C) this obliteration is efiected. In
Anodon, besides being thickened, the skeletal substance of
the filament develops a specially dense rod-like body on
each side of each filament. Although the structure of the
ctenidium is thus highly complicated in Anodon, it is yet
more so in some of the Siphon.ite genera of Lamellibranch-s.
The filaments take on a secondary grouping, the surface of
the lamella being thrown into a series of half-cylindrical
ridges, each consisting of ten or twenty filaments ; a filament
XVI. — 67
6.9Q
MOLLUSCA
[LAilEIXraRANCHUL
of much greater strength and thickness than the others may
be placed between each pair of groups. In Anodon, as in
and to one anolher. A shows tv/o conditions with free giU-axis ; B,
ditioD at foremost region in Anodon ; C, hind region of foot in Anodon ; D,
legion altogether posterior to the foot in Anodon. a, visceral mass ; h, foot ;
c, mantle flap ; d, axis of gill or ctenidiuni ; c, adaxial lamella of outer gill-
plate : er, reflected lamella of outer gill-plate ; / adaxial lameUa of inner
gill-plate ; fr, reflected lamella of inner gill-plate ; g, line of concrescence of
tlie reflected lamellfs of the two inner gill-plates ; h, rectum ; i, supra-branchial
space of the svib-pallial chamber. (Original.)
many other Lamellibrancbs, the ova and hatched embryos
are carried ior a tinie in the ctenidia or giU apparatus, and
in this particular case the space between the two lameDse
Fio 136 — T- -i^\ r fit cti n nf 0 e filter gill plnt^ nf TVeUiena pohimorpha
(after He li-tan I*cck), /, constituent gill filaments , /, fibrous sub epidermic
tissue; eh, oliitoni^us substance of the filaments; ncA, cells related to the
cliitonons substjinco ; lac, lacunar tissue ; pip, pigment-cells ; be, blood-
corpusclcii ; Je, frontal oplthoHum ; (/«', Ife", two rows of latero-frontal epi-
thelial cells with long cilia ; Ir/, fibrous, poscibly muscular, substance of tJie
later-dlamentcr juncltons.
of the outer gill-plate is that which serves ij receive the
ova (fig. 1 37, A). The young are nourished by a substance
formed by the ceils •which cover the spongy inter-U;mel]2.r
outgrowths.
There are certain other points in the modification of the
typical ctenidium which must be noted in order to under-
stand the ctenidium of Anodon. The a-s'is of each ctenid-
ium, right and left, starts from a point well forward near
the labial tentacles, but it is at first only a ridge, and does
not project as a free cylindrical axis until the back part of
Fio. 137.— Transverse sections of gill-plates of Anodon (after PeClc). A. Outer
gill-plate. B. Inner gill-plate. C. A portion of B more highly magnified.
c.l, outer lamella; i.^ inner lamella; v, blood-vessel: /, constituent fila-
ments ; tuc, lacunar tissue ; cA, chitonous substance of the filament ; cAr,
chitouous rod embedded in the softer substance eft.
the foot is reached. This is difficult to see at all in Ano-
don, but if the mantle-.skirt be entirely cleared away, and
if the dependent lamella; which spring from the ctenidia'
axis be carefully cropi)ed away so as to leave the axis itsell
intact, we obtain the form shown in fig. 131, where ^ and
h are re.spectively the left and the right ctenidial axes pro-
jecting freely beyond the body. In Area this can be seen
with far le.ss trouble, for the filaments are more easily re-
moved than are the consolidated lamella; formed by the
filaments of Anodon, and in Area the free axes of the
ctenidia are large and firm in textm'6 (fig. 132, <•, d).
If we were to make a vertical section across the long
axis of a Lamellibranch which had the axis of its ctenidium
free from its origin onwards, we should find such relations
as are shown in the diagram fig. lo3, A. The gill axis d
is seen Ijing in the sul>pallia! chamber between the foot
b and the mantle c. From it depend the gill-filaments or
lamelliB — formed by united filaments — drawn as black lines
/. On the loft side these lamell;c are represented as hav-
ing only a small reflected growth, on the right side the
reflected ramus or lamella is complete (fr and er). The
actual condition in Anodon at the region where the gills
commence anteriorly is shown in fig. 135, B. The axis of
the ctenidium is seen to be adherent to, or fused by con-
crescence with, the body-wall, and moreover on each side
the outer lamella of the outer gUI-plate is fused to the
mantle, whilst the inner lameUa of the inner gill-plate is
fused to the foot. If we pass a 'little backwards and take
another section nearer the liinder margin of the *"ot, wa
LAMZLLIBR ANCEU. ]
M 0 L L U S C A
691
get the arrange'nent shown diagrammatically in fig. 135,
C, and more correctly in fig. 142. In this region the inner
Jamellse of the inner gill-plates are no longer affixed to the
foot. Passing still further back behind the foot, we find
Tie. 138. — GiU-Tamellse of Anodon ^fter Peck). A. t'ragment of the enter
Uihclla of an inner giU-plate torn u-om the coilnected inner lamella, the aab-
flLimentar tissue also partly cut away round the edges so as to expose the
filaments, their transverse junctions ^r, and the "windows" left in the lattice-
work ; ife, internal surface of the lamella ; V, vessel. B. Diagram of a block
cut from the outer lamella of the enter gill-plate and seen irom the inter-
lamellar surface fafter Peck). / constituent tilamenta ; trf, ilbrous tissue of
the transverse inter-filamentar junctions ; v, blood-vessel ; ilj, inter-lamellar
Junction. The series of oval holes on the back of the lamella are the water-
pores which open bet\7een the illaments in irregular rows separated horizon-
tally by the transverse inter-filamentar junctions.
in Anodon the condition shown in the section D, fig. 135.
The axes t are now free ; the outer lamellae of the outer
gill-pIates (^c)' still adhere by concrescence to the mantle-
skirt, whilst the inner lamellaa of the inner gill-plates meet
one another and a »
fuse by concres- y^ "\
cence at ff. In //ni^ jt»\ /^ ^\
the lateral view of (j
the animal with
reflected mantle- ' i ib'\ i^ hii i \
skirt and gill- \\« \y "11 * :r-—^
plates, the line of
concrescence of the ,
. „ - Fro. 139.— Transverse sections of ^, a Lamellibranch,
inner lameUse Ol and B, an Isopleurous Gastropod (Chiton), to show
thft innpr mil- the relations of jj, the foot ; &r, the branchiae : and
' , . ^,rr m, the mantle. (From Gegenbaur.)
plates 13 readily
seen; it is marked aa in fig. 124, (.5). In the same
figure the free part of the inner lamella of the inner
gOl-plate resting on the foot is marked s, whilst the
attached part — the most anterior — has been snipped
with scissors so as to show the genital and nephridial
apertures x and v. The concrescence, then, of the
free edge of the reflected lamelise of the gill-plates of
Anodon is very extensive. It is important, because such
a concrescence is by no means universal, and does not
occur, for example, in Mytilus or in Area ; further, because
''W ^"
when its occurrence ;.^ o.-.ce appreciated, the reduction of
the gill-pIates of Anode a to the plume-typa of the simplest
ctenidium presents no difficulty; and, lastly, it has import-
ance in reference to its physio- . . .
logical significance. The me- "'-^
chanical result of the concres-
cence of the outer lamellae to
the mantle-flap, and of the
inns? lamellcs to one another
as shown in section D, fig.
135, is that the sub-pallial ''""
space is divided into two m'-r ^
spaces by a horizontal sep- Fio. UO Lateral view of a Moctra,
turn Thfl iirmor ^nacR li\ the right valve of thashell and right
lum. ine upper space [l) „,r.ntlc.aap removed, and the si-
COmmUnicateS with the outer phons reh-acted. br, br', outer and
1 J 1. ii, . inner gill-piates ; (, labial tentacle ;
world by the excurrent or SU- to, ;,-, upper .-vnd lower siphons ; ms,
perior siphonal notch of the siphonal muscle of the mantle-aap ;
1 /£ 1 n i j\ 11 ""' ^n'firior aaductor muscle ; mp,
mantle (ng. 124, «); the lower posterior adductor muscle ; p, foot ;
space communicates by the '• '™'«- C^om Oeaenb^ur.)
lower siphonal notch (e in fig. 124). The only communica-
tion between the two spaces, excepting through the treliis-
work of the gill-plates, is by the slit (s in fig. 124, (5)) left
by the non-concrescence of a part of the inner lamella of the
inner gill-plate with the foot. A probe (17) is introduced
through this slit-like passage, and it is seen to pass out by
the excurrent siphonal notch. It is through this passage,
or indirectly through the pores of the gill-plates, that the
water introduced into the lower sub-pallial space must pass
on its way to the excurrent siphonal notch. Such a
subdivision of the pallial chamber, and direction of the
Fio. 141.— The same animal as flg. 140, • i ' -nd siphons expanded.
Letters as in flg. 140. (F -or.i Gegenbaur.)
currents set up within it do not exist in a number of
Lamellibranchs which have the giU-lameUse comparatively
free (Mytilus, Area, Trigonia, &c.), and it is in these forms
that there is least modification by concrescence of the pri-
mary filamentous- elements of the lamellae. Probably the
gill -structure of Lamellibranchs will ultimately furnish
some classificatory characters of value when they have
been thoroughly investigated throughout the class.
The alimentary canal of Anodon is shown in fig. 124, (4).
The mouth is placed between the anterior adductor and
the foot ; the anus opens on a median papilla overlying
the posterior adductor, and discharges into the superior
pallial chamber along which the excurrent stream passes.
The- coil of the intestine in Anodon is similar to that of
other Lamellibranchs, but the crystalline style and its
diverticulum are not present here. The rectum traverses
the pericardium, and has the ventricle of the heart wrapped,
as it were, around it. This is not an unusual arrangement
in Lamellibranchs, and a similar disposition occurs in some
Gastropoda (HaUotis). A pair of ducts (ai) lead from the
first enlargement of the alimentary tract called stomach
into a pair of large digestive glands, the so-called liver,
the branches of which are closely packed in this region
(n/). The food of the Anodon, as of other Lamellibranchs,
consists of microscopic animal and vegetable organisms,
which are brought to the mouth by the stream which sets
into the sub-pallial chamber at the lower siphonal notch
(e in fig. 124). Probably a straining of water fiom solid
C9i
M O L L U S C A
[l Asnxi.nsR a:s' ohlv.
particles is effected by tLe latt?.ce-wcrk of the ctenidia cr
gi!l-plates.
The heart of Anodon consists of a median ventricle em-
bracing the rectum (fig. 143, A), and giving ofi'an anterior
and a posterior o.rtory, and of two auiicles which open into
the ventricle by orifices protected by valves.
The blood is colourless, and has colourleE.^ amoeboid
corpuscles floating in it. In two Lamellibranchs, Solen
(Ceratisolen) hgumen and Area Koie, the blood is crimson,
owing to the presence of corpuscles impregnated with
hjemoglobin (Lankester, 31). In Ajiodon the blood is
driven by the ventricle through the arteries into vessel-
like spaces, wliich soon become irregular lacunae surround-
ing the viscera, but in p.irts — e.ff., the labial tentacles and
walla of the gut — verj' fine vessels with endothelial cell-
lining are found. The blood makes its way by large
veins to a venous sinus which lies in the middle line be-
low the heart, having the paired rentil organs (nephridia)
placed between it and that organ. Hence it passes
through the vessels of the glandular walls of the nephridia
right and left into the gill-lamella:, whence it returns
through many openings into the widely-stretched auricles,
A great deal more pre-
cision TnR been given to
accounts of the structure
of arteries, veins, and
capillaries in Anodou
than the facts warrant.
The course of tho blood-
stream can only be somt-
wbat vaguely inferred ex-
cept in its largest out-
lines. Distinct arterial j.
and venous channels can-
not be distinguished iii
the gill-lamelite, in spite
of what Langer (58) has
written on the subject,
though it is highly prob-
able^ that there issome j.,^ n2._verti„i section throneh ^ Ano-
land of circulation m the doiita,ataut the mid-region of the toot, m,
cril's Tn ttiA filiiTipnta nmntle-ftap ; br, outer, 6V, inner gill-plate
glUS. in ine niamentS _eachcociposcdoffr«-ol!imellEe;/,foot; t>,
of the gill of Mytiius the wntncle of the heart ; a, anricle ; y, p\
. 1 , ^ .^_ . J. .1 J pericardii; cavity ; I, intestine.
tubular cavity is divided
by a more or less complete fibrous septum into two
channels, presumably for an ascending and a descend-
ing blood-current. The ventricle and auricles of Anodon
lie in a pericardium which is clothed with a pave-
ment endothelium (d, fig. 143). Veins are said by Keber
and others to open anteriorly into it, but thii appears to
be an error. It does not contain blood or communicate
directly with the blood-system ; this isolation of the peri-
cardium we have noted already in Gastropo<U and Cephslo-
pods. A good case for the examination of tho quciition as
to whether blood enters the pericardium of Lamellibranchs,
or escapes from the foot, or by the renal organs when the
animal suddenly contracts, is furnished by the Solen Ice/u-
men, which has red blood-corpuscles. According to ob-
servations made by Penrose (53) on an uninjured Solen
leffMmen, no red corpuscles are to be seen in the pericardial
space, although the heart is filled with them, and no such
corpuscles are ever discharged l)y the animal when it is
irritated.
The pair of nephridia of Anodon, called in Lamelli-
branchs the organ of Bojanus, lie below tlie membranous
floor of the pericardium, and open into it by two well-
marked aportm-es (e and/ in fig. 143). Each nephridium,
after being bent upon itself as shown in fig. 143, C, D,
opens to the exterior by a pore placed at the point marked
X in fig. 124, (5), (6), It is no doubt possible, as in the
Gastropoda and Cephalopoda, for water to enter frcr:: the
exterior by the nephridia into the pericardium, but that
it ever does so is as yet not proved. What is certain
from the set of the ciliarj- currents is that liquid generally
J,- 3
Fin. 143. — Diagraina showing the lelatiors of pericardium end LcrihriOIa;:. a
LdmaUibranch such as Anodon. A. Peiicardium opened doisjjly eo a^ to
expose the heart and the floor of the pericardial chamber d. B. Hcirt
removed and floor of the pericardium cut away on the left side so as to open
the non-glandular sac of the nephridium, exposing the glandular eac 6,
which is also cut into eo as to show the probe /. C. Ideal pericardium anil
nephridium viewed laterally. D. Lateral view showing the actual relation
of the glandul.1T and non-glandular sacs ol the nephridium. The arrows
indicate the course of fluid from the pericardium oucwards. c. ventricle «f
the heart ; h, auricle ; 6b, cut i-emnant of th-3 a-,iricle ; c, dorsal wall of tho
pericardium cut and reiiccted ; e, reno-pericardicl ori3ce ; /, probe inti'O-
duced into the left reno-pericsrdial oriCce ; ff, non-glanduloT sac of the loft
nephridium; A, glandular sac of the left nephridi'jm; i, pcre leading £:om
the glandular into the non-glandular sac of the left nephridium; k, por«
leading from the non-glandular sac to the e,xterior ; ac, anterior, ab, po.stenor,
cut r
nts of the intestine and ventricle.
passes out of the pericardium by the nephridia. One half
of each nephridium is of a dark-green colour and glandular
(h in fig. 143). This opens into the reflected portion which
overlies it as shown in the diagram fig. 143, D, t ; the latter
has non-glandular walls, and opens by the pore k to the
exterior. The nephridia may be more ramified in other
Lamellibranchs than they are in Anodon. In some they
are difiicult to discover. That of the conmion oyster
has recently (1882) been detected by Hoek (54), Each
nephridium in the oyster is a pjTiform sac, which commu-
nicates by a narrow canal with the urino-genital groove
placed to the front of tho great adductor muscle ; by a
second narrow canal it comm.unicates with the pericardium.
From all parts of the pyriform sac narrow stalk-Uke tubes
are given off, ending in abundant widely-spread branching
glandular caeca, which form the essential renal secreting
apparatus. The genital duct opens by a pore into tho
uriuo-genita! groove of the oyster (the s^.me Arrangement
being repeated on each side of tho body) close to but distinct
from the aperture of the ncphridial canal. Hence, except
for the formation of a urino-genital groove, the apei-tures
are placed as they are in Anodon. Previously to Ht>ek'*
discovciy a brown-coloured investment of the aiiricles of
tho heart of the oyster had been supposed to represent
tho nephridia in a rudimentary state. This icvcstiucnt,
which occurs also in Mytiius but not in Anodon, may po.^-
sibly consist of secreting cells, and may be comparable t.^
tho pericardial accessory glandular growths of Cephalopoda.
Jfervous Syslem and Seme-orr/atis. — In Anodon then- art-
three well-developed pairs of nerve-ganglia (fig. 144, B and
fig. 1 24, (6)). An anterior pair, lying one on each side of tho
OAKELLIBRAJiCHlA.
mouth (fig. 144, B, a) and connected in front of it by a
commissure, are the representatives of the cerebral, pleural,
and visceral ganglia of the typical Mollusc, which axe not
here diiierentiated as they are in Gastropods (compare,
however, fig. 67). A pair placed close together in the foot
(fig. 144, B, 5, and fig.
124, (6), cur) are the typ-
ical pedal ganglia ; they
are joined to the cerebro-
pleuio - visceral ganglia
by connectives.
Posteriorly beneath
the posterior adductors,
and covered only by a
thin layer of elongated
epidermal cells, are the
olfactory ganglia, their
epidermal clothing con-
stituting the pair of os-
phradia, which are thus
seen in Lamellibranchs
to occupy their typical
position and to have the
typical innervation,- — the
MOELUSCA
693
lUm beine given off by Teredo ; B, ot Asodonta ; C, of Pecten.
,* . "^ ,° ,. "^ cerebral ganglion-pair (=cerebro-pleui'o-
ttie visceral ganglion vlsceraJ) ; t, pedal ganglion-psir ; c, olfac-
that is to say, by the tory (oaphratfia!) ganglion-paij.
•undifferentiated ,cerebro-pleuro-visceral ganglion of its
proper side. This identification of the posterior gangliou-
,paii' of Lamellibranchs is due to Spengel (11).. Othej
Fio. 145. — PalJial eyo of Spondylna (from Hlckson). a, pwB-corneal epithe-
fip^n ; b, cfiUnlar lens ; c, retinal body ; d, tapetam *, e, pigment ; / '.■etinal
nerve ; g, complementary nerve ; h, epithelial cells fllled with "pi^ent ; k,
tehtacle
anatomists have considered this ganglion-pair as corre-
sponding to either the pleural or the visceral of Gastropoda,
or to both, and very usually it is termed "the parieto-
splanchnic" (Huxley).
The sense-organs of Anodon other than the osphradia
consist of a pair of otocysts attached to the pedal ganglia
{fig. 124, (6), ay). The otocysts of Cyclas are peculiarly
favourable for study on account of the transparency of the
small foot in which they lie, and may be taken as typical
of those of Lamellibranchs generally. The structure of
one is exhibited in fig. 146. A single otolith is present
as in the veliger embryos of Opisthobranchia. In adult
Gastropoda there are frequently a large number of rod-like
tjtoliths instead of one.
Anodon has no eyes of any sort, and the tentacles on the
mantle edge are limited to its posterior border. This
ieficiency is very usual in the class; at the same time, many
Lamellibranchs have tentacles on the edge of the mantle
supplied by a pair of large well-developed nerves, which
are gi ven off from the cci'ebro-pleuro- visceral ganglion-pair,
Fia. 146. — Otocyst
and very frequently some of these tentacles have undergone
a fecial metamorphosis converting them into highly-
organized eyes. Such eyes on the mantle-edge are found
in Pecten, Spondylus, Lima, Ostrea (?), Pinna,, .Pectxmculus,
Modiola, Mytilua ('!), Cardium, Telhna,
Mactra, Venus, Solen, Pholas, and Qa-
leomma. They are totally distinct from
the cephalic eyes of typical Moliusca, and
have a different structure and historical de-
velopment. They have not originated as
pits but as tentacles. They agree with the ,
dorsal eyes of .Onchidium (Pulmonata) in of Cycias^\&oi
the curious fact that the optic nerve pene- ^^ni^'^^^iiiatM
trates the capsule of the eye and passes in cells lining the
front of the retinal body (fig. 145), so that °'"°' °' °*°"'''-
its fibres join the anterior faces of the nerve-end cells as
in Vertebrates, instead of their posterior faces as in. the
cephalic eyes of Moliusca and Arthropoda ; moreover, the
lens is not a cuticular product but a cellular structure,
which, again, is a feature of agreement vrith the Vertebrate
eye. It must, however, be distinctly borne in mind that
there is a fundamental difference between the eye of Verte-
brates and of all other groups in the fact that in the
Vertebrata the retinal body is itself a part of the central
nei-vous system, and not a separate modification of the
epidefmis — -myelonic as opposed to epidermic. The struc-
ture of the reputed eyes of several of the above-named
genera has not been carefully examined. In Pecten and
Spondylus, however, they have been fully studied (see fig.
145, and explanation).
The gonads of Anodon are placed in distinct male and
female individuals. In some Lamellibranchs — for instance,
the European Oyster and the Pisidium pusillum — the sexeS
are linited in the same individual; but here, as in most
hermaphrodite animals, the two sexual elements are not
ripe in the same individual at the same miomeut. It has
been conclusively shown that the Ostred edulis does not
fertilize itself. The American Oyster (0. virginiana) and
the Portuguese Oyster (0. angxdcUa) have the sexes sepa-,
rate, and fertilization is effected in the open water after
the discharge of the ova and the spermatozoa from the
females and males respectively. In the Ostrea edulis fertil-
ization of the eggs is effected at the moment of their escape
from the uro-genital groove, or even before, by means of
spermatozoa drawn into the sub-paUial chamber by the in-
current ciliary stream, and the embryos pass through the
early stages of development whilst entangled between the
gill-lamelhe of the female parent (fig. 6). In Anodon the
eggs pass into the space between the two lamellae of the
outer gill-plate, and are there fertilized, and advance whilst
A r., _ B
•j>-a4
Fio. 147. — Two stages in the development of Anodonta (from Balfour). Both
tlgilres_ represent the glochidium stage. A. when free swimming, shows t^
two dentigerons valves widely open. B, a later stage, afttr ftxture to the fla
of a fish. 9h, shell ; ad, adductor muscle ; », teeth of the shell ; 6^, byssiu ;
a.ad, anterior addnctor ; p.ad, posterior adductor ; m(, mantle-flap ; / foot ;
br, branchial filaments ; au.t>, otocyst ; aX, alimentary canal.
still in this position to the glochidium phase of develop^
ment (fig. 147). They may be found here in thousands)
in the summer and autumn months. The gonads them^
selves are extremely simple arborescent glands which open
to the exterior by two simple ducts, one ri^ht and ont
694
MOLLUSCA
[LAilELLrBEAJfC3
left, contitftioua with the wall of the tubular branches of
the gland (fig. 124, (5), (6), y). In no Lamdlibiunch is
there a divergence from this structure, excepliiig that ia
some (Ostrea) the contiguous nephridial and the genital
aperture are sunk in a m-ino-gcnital ((jroove, v/hich in other
cases (Spondylus ?) may partiaUy close up so as to con-
stitute a single pore for the nephridial and genital ducts.
No accessory genital glands are present.
The development of Anodon is remarkable for tho curious
larval form known as Glochidimn(f'2. 147). The Glochidium
Pig. 148. — Embryos of Pisidium pjw.7h!m (after Lanbester). A. Only foar
embryoDic cells flxe preseot, still encloaed in the epg envelope. B. The cells
have multiplied aatl commencsd to invugiaate, formins a blastopore or oriflce
of invagination, M.
quits the gill-pouch of its parent and Bwims by alternate
opening and shutting of tho valves of its shell, as do
adult Pecten and Lima, trailing at the same time a long
Fig. 150.
Fio. 140.— Embryo of PisWium pusilhtin in the di jtula stage, surface view
(after Lajiko3ter). The embryo has increased in size by accumulation of
liquid bctweea the outer and tho Invaginatca cells. The blastopore has
closed.
Flo. l&O. — B. Same embryo na flfj. 140, In optical metllan eection, showinjj the
invaylnated cells fty which form tho arch-enterc.n, and tho mesoblastic ceils
mt wliich arc budded olf from the nurfaca of tlio mass ftu, and apply them-
BOlvci: to tho inner surface of tlio dtric or epiblaicic cell-layer ep, C. The
same embrj'o focused so na to show the mesoblastlc ceils which immediately
uiidc.-lie the outer celMaycr.
byssus thread. By this it is brought into contact with the
fin of £, fich, exMii a:3 Tcich, Stickleback, or others, and effects
a hold thereon by means of the toothed edge of its shells.
Hera it beccinc-3 encysted, and is nourished by the exuda-
tions of the fish. A distinct devebpiaent of its internal
organs has been tvacsd by the lato Professor Balfour, bvit no
one has followed it to the moment at which ii diop.'i from
the fish's fin and assumes the form of shell characteristic of
the parent. Other LaineUibranche exhibit either a trocho-
sphere larta \rJiich becomes a Yeliger, differing only from
tho Gastropod's and Pteropod's Veliger in haviug bilateral
shell-calcifications instead of a single central one ; or, like
Anodon, they may develop within tho gill-plates of the
mot.'ior, though without presenting such a specialized larva,
as the Glochidium. An example of the former is seen in the
Fio. 151. — Further stpges in tho develop^ncnt cf Pi
Lankester). A. Optiail section of an embryo in which the foot h-is b^^-jn V
develop. B. The same embryo focased to its surface plane to.^Lj.v t..
moutli 0. C. Later embryo, showing the sbeU-glnnd Sj"). D. Lateral vlciv < [
the same eral-ryo. E. Later stage, withrudimonta of the mantle-flap, latvr.i
view. P. Still later stage, with sheU-valves and branchial filameiils. r;-
epiblast; me, mcsoblast; (d, mot-enteron ; rp, rectal peduncle or pedicle o:
invagination connecting the met-cntoron with the cicfCrix of the bUstopore ,
0, mouth; p/i, piiaryux ; s\ shell-eland; n;?i, mantle-flap; &r, braachiai
filaments ; y, granular cells of doubmil signiflcance ; f, vesicular structlir-
of unknown eignillcaucc.
development of the European Oyster, to the figure of whiol
and its explanation the reader is specially refen-ed (iig. 6;.
.An example of the latter is seen in a common iKtlc
fresh-water bivalve, the Pisidimn pusilhim, which has been
studied by Lankester (12). The successive stages of tlie
development of this Lamellibranch are illustrated ia the
woodcuts figs. 148 to 153 inclusive. These should be
compared with the figure."* of " Gastropod development
(figs. 3, 4, 5, 7, and 72**»), Fig; 143 shovrs tho cleavage
-of tho cgg<ell into four (A); and at a later stage the tucking
in of seme of the cells, to form an iijvaginated series (£),
M O L — M O L
695
The embryonic cells continue to divide, ana form an oral
vesicle containing liquid (fig. 149); within this, at one pole,
13 seen the mass of invaginated cells (fig. 150, hi/). These
invaginated cells are the arch-enteron ; they proliferate and
give oflf branching cells, which apply themselves (fig. 150,
C) to the inner face of the vesicle, thus forming the meso-
ViO. 152.— Diagram of embryo of Pisidiuin in tlio same stago as E in fig. T51.
m, mouth ; /, foot ; ph, pharynx ; gs, met-enteron ; pi, rectal pedunclo OF
pcdicl« of invagination ; siu, shell-gland. (Prom Lankcster.)
blast or coelomic outgrowths. The outer single layer of
cells which constitutes the surface of the vesicle (fig.
147) is the ectoderm or epiblast or deric cell-layer. The
little mass of hypoblast or
J^xf
enteric cell-mass now
largea, but remains con-
nected with the cicatrix of
the blastopore or orifice of
invagination by a stalk, the
rectal peduncle (fig. 151, A,
rpy. The enteron itself be-
comes bilobed ajid is joinel
by a new invagination, that
of the mouth and stomo-
ds2ura, ph. Fig. 151, E
shows the origin of the
mouth o, being a deeper
view of the same specimen. Fio.iss.—Dia^amorcmbryootPisidium,
,v -,• V* r. in same stage as r in fig. 151 (after Lau-
la the same position -wmcn kester). r.i,iuouth ; x, anus; /, foot; ftr,
is drawn in fig. 151, A. branchial filaments ; mn margin of the
° , . !• mantle-skirt •£, organ of Bojanu3(ne-
The meSOblast multipliea 'phridiuin_). The unshaded area gives
its cells, which become the position of the sheU-valre.
partly muscular and partly skeleto-trophic. Centro-dor-
sally now appears the embryonic shell-gland (fig. 151,
C, fk). The pharynx or stomodaeum is still small, the
foot not yet prominent. A later stage is seen in fig.
152, where the pharynx is widely open and^tlie foot pro-
minent. No ciliated velum or prie-oral (cephaUc) lobe
ever develops. The shell-gland disappears, the mantle-
skirt is. raised as a ridge (fig. 151, E, mn), the paired
shell-valves are secreted, the anus opens by a proctodasal
Ingrowth into the rectal peduncle, and the rudiments of
the gills (br) and of the nephridia (B) appear '^figs. 151,
F, and "153, dorsal and lateral views of same stage), and
thus the chief organs and general form of the adult are
acquired. Later changes, not drawn here, consist in the
growth of the shell-valves over the whole area of the
mantle-flaps, and in the multiplication of the giU fila-
ments and their consolidation to form gill -plates. It
is important to note that the gill-filaments are formed
one by one pocteriorlt/. The labial tentacles are formed
late. In the allied genus Cyclas, a byssus gland is formed
in the foot and subsequently disappears, but no such gland
occurs in Pisidium. The nerve-ganglia and the otocysts
probably form from thickenings of the epiblaat, but detailed
observation on this and other points of histogenesis in the
Lamellibranchia is still wanting.
List of Memoirs, £c., referred to by numbers in Vic preceding article.— O) G.
Cuvier, Memoires pour urvir a l'histoir« et d I'anatomie dca Mollusques, Paris,
1816. (2) J. Poll, Testacea ■utrivsque Sicilias, eorumque historia et anatomy,
tahutis aeneis 49 illustratOy vols. i.-Jii., fol., Parma, 1791-1795 and 1826-1827.
(3) St delle Chi^e, Memorie suila storia t iwioxia tfcpli aiiinwit unia vert^hre
del regno di ^apoli, Naplea, 1823-1829; new edit withl72 plates, fol., 1S43.
(4) J. Vaughan Thompson, Zoological Ri-smrJies, Cork, 1S30 ; memoir iv., "On
the Cirripedes or Barnacles, demonstrating their deceptive character." (B) A.
Kowalewsky, "Entwjckelungsgeschichte der einfachen Ascidien," in Mivn. <*«
r^cad. des Sciences de St HUrsbourg, 18ti6, and "Entwickeliingsgescbichfe
des Amphiosms lanceolatus," ibid., 1867. (6J J. Vaugban Thompson, Zoological
Researches, Cork, 1830; memoir v., "Polyzoa, a new animal discovered as
an inhabitant of some Zoophytes." (7) C. G. Ehrenberg, Die Eoralleiukitn d-.s
Rothcn Mecres, Berlin, 1834 {Abhand. d. lu Akad. d. Wissenschaflen t:i Berlin,
1S32). (8) H. Milne-Edwards, Sechcrclies anatoiii.tques physiologimus et zool'--
giques Eur Us Polyviers de France, Paris, 1841-1844. (9) W. H. Caldwell, "Oj
the development of Phoronis," Proc. Hoy. Soc., 1882. (10) Richard Owen, Memo.:-
on the Pearly Nautilus, London, 1832. (U) T. H. Huxley, " On the morpholoev
of the cephalou3 Molliisca," Phil. Trans., 1853. (12) E. Ray Lankester, "Cou-
tributions to the developmental history of the Jlollusca," Phil. Trans., 1875.
(13) E. Ray Lankester, "Notes on Embryology and Classification," Qvcrt.'
Journ. Microsc. Sc, 1877. (14)''J. Carriere,"Das ■Wassergefass-Syst^md. Lauislii-
branchiaten u. Gaatropoden, " Zoolog. Anzciger, 1881, No. 90. (lii) B. Rrty
Lankester, " Development of the Pond-Snai'.," Quart. Journ. Microsc. Sc, 1874,
and "SheU-gland of Cyclas and Planula of LinmBeus," ibid., 1876. (16) E.
Horst, "Development of the European Oyster," Quart. Journ. Microsc. Sr..,
1S82, p. 341. (17) E. Ray Lankester, "Coincidence of the blastopore and
anus in Paludina," Quart. Journ. Microsc. Sc, 1876. ^18) Id., "Zoolosical
Observations made at Naples," Anttals aiwi Mag. Nat. hist., February, 1S73,
(19) W. K. Brooks, " Development of the American Oyster," lUport of the
Commissioners of Fisheries of Maryland, 18£0. (20) Henri Milne-Ed warxls,
Papers in the Annates des Sciences Naturelks, 1S41-1860. (ZL) H. de Lacaze
Duthiers, Papers in the 4nncUes des Sciences NatureV.cs, e.g., *' Anemia" (1854),
"Mj-tilus"(1856),"Dentalium"(1856,18S7),"Purpura"(1869),"Haliotis"(18i9),
" Vermetus" (1860). (22) A. Kolllkor, Bntwickelungsgeschickle dcr Cephalopoden,
Zurich, 1844. (23) C. Gegenliaur, Untei-iftchungen iiber Pteropoden vnd Hetirc-
poden, L/eipsic, J855. (34) J. W. SpcngeH/' Die Geruchsorgane und das Neiven-
eystem der MoUusken," Zeitschr. f. vnss. Zool.', ISfil. (25) A- A. W. Hubrecht,
"On Proneomcnia SJiuUrt nov. gen. et sp., witli remarks upon the anafODiy
and histology of the Amphineura," Niederldndisckes Archivfiir ^oologie, supple-
ment volume, 1831. (28) Adam Sedgwick, "On certain points in the anatomy
of Chiton," Proc Roy. Soc. Lond., 1881. (27) E. Ray Lankester, "On some
undescribed points in the anatomy of the Limpet," Annals aiul Maq. Nat,
History, 1867 ; J. T. Cunningham, " The Renal Organs of Patella," Quart.' Journ.
Microsc. Sc, 1883. (23) P. Fraisse, " Ueber MoUuskpnaugen mit cmbryonalcm
Tynus," Zeitschr. /. \oiss. Zool.; 1831.. (29) L. v. Graif, " Ueber Rhodope Vcranii,
Kbll.," Morpholog. Jahrb., voL viii. (30) H. Simroth, "Das FassDcn-engystem
der Paludina vivipara," Zeitschr. f. xoiss. Zool., 1881. (31) E. Ray Lankestei",
"A contribution to the knovrledge of Haemoglobin," Proc. Roy. Soc Lond.,
1873. (32) H. de Lacare Duthiers, "Du syst^me ner\'eux dea MoUiisciues
Gasteropodes Pulmones aquatiques et d'un nouvel organe d'innen'ation," j4rcA,.
de Zoologit expcrimenUile, voL i. (33) C. Semper, Animal Life (for eye 'of
Onchidium, p. 371), International Scientific eeries, 1881. (34) Same as number
18. (35) E. Ray Lankester, " Observations on the development of the Cep!mlo-
poda. Quart. Journ. Microsc Sc, 1875. (36) J. Tan der Hoeven, "Bijdrage
tot de outleedkuudige kennis aangaaende Nautilus pompilivs," Verhandl. d.
K. Alxid. V. Wet. Naiurk., Amsterdam, 1850. (37) B. Kay Lankester and A. G.
Bourne, " On the existence of Spengel's olfactory organ and of paired geuitil
ducts in the Pearly Nautilus," Quart. Journ. Microsc. Sc, 1883. (38) J. VT.
Vigelius, "Ueber das Bxci-etions-Syalera der Cephalopoden," JViederldnrfiscAw
Archiv fur Zoologie, bd. v., 1880. (39) Albany Hancock, "On the nervous
system of Ommastrepkes todariis," Anncls and Mag. Nat. Hist., 1852. (40)
J. D. Macdonald, "On the anatomy of Nautilus umbilicatus," Phil. 2'rans. v)
Roy. Soc. Lond., 1S55. (41) V. Hcnsen, " Ueber das Auge einiger Cephalopoden,"
Zeitschr. f. wlss. Saol., 1865. (42) A. d'Orbigny, Mollusques vivants et fossiUs,
t. i. (Cephalopodes acetabuUfferes), Paris, 184& (with 36 plates). (43) Bobretzky,
"On the development of the Cephalopoda," Trans, of Soc of Friends of Nat.
Hist, of Moscow, vol. xxiv. (Russian). (44) T. H. Huxley, "Oviducts of the
Smelt," Proc Zool. Soc Lond., 1883. (45) Same as 35. (46) P. M. Balfour,
Comparative Embryology, vols. i. and ii., London, 1881-1882. (47) H. Gries-
bach, " Ueber das GefiUis-System und die Wasserauftiahme bei den N^adcn uud
Mytiliden," Zeitschr. f. u'Us. Zool., 1883. (48) Same as 14. v49) Same as iS.
(50) R. Holman Pecl^ "The Btnictare of the Lamelli branchiate gill," Quart.
Journ. of Microsc. Sc, 1876. (51) K. Mitsukuri, "Structure end signiiicance
of some aberrant forms of LameUi branchiate gil\a,"'Quart. Journ. Microsc. Sc,
1881. (52) K. Langer, "Das Gefass-System der Teichmussel." Denk. k'.iii.
Akad. d. iVisscnsch., Vienna, 1855-1856. (53) J. Penrose, in "Report of the
Committee on the Zoological Station of Naples," British Assoc Report, 18S2.
(54) P. P. C. Hoek, "l/cs orgaues de la generation de Thuitre," Journ. de la Soc
Neerlaniaise de Zool., 1883.
(£. R. L.)
MOLLUSCOIDS. ' See Brachiopoda and Polyzoa.
MOLOCH, or Molech — in Hebrew, with the doubtful
exception of 1 Kings xi. 7, always "Hjisn with the article-
in the last ages of the kingdom were wont to propitiate by
the sacrifice of their own children. The phrase employed
in speaking of these sacrifices is "to make one's son or
is the name or title of the divinity which the men of Judah | daughter pass through fire to the Moloch " (2 Kings xxiii
696
M O L — M O L
10; Jer. zxxii. 35, and so without the words "through fire"
Lev. xviii. 21); but it appears from Ezek. xvi. 20, 21
that this phrase denotes a human holocaust,'- and not, as
sometimes has been thought, a mere consecration to Moloch
by passing through or between fires, as in the Roman Palilia
and similar rites elsewhere. Human sacrifices were com-
mon in Semitic heathenism, and at least the idea of such
sacrifices was not unknown to Israel in early times (Isaac,
Jephthah's daughter), though in the sunny days of the
nation, when religion was a joyous thing, there is no
reason to think that they were actually practised.- It
was otherwise in the neighbouring nations, and in par-
ticular we learn from 2 Kings iii. 27 that the piacular
sacrifice of his son and heir was the last offering which
the king of Moab made to deliver his country. Even the
Hebrew historian ascribes to this act the effect of rousing
divine indignation against the invading host of Israel ; it
is not, therefore, surprising that under the miseries brought
on Palestine by the westward march of the Assyrian
power, when the old gladness of Israel's faith was
swallowed up in a crushing sense of divine anger, the idea
of the sacrifice of one's ovm son, as the most powerful of
atoning rites, should have taken hold of those kings of
Judah (Ahaz and Manasseh, 2 Kings xvi. 3, xxi. 6) who
were otherwise prone, in their hopelessness of help from
the old religion (Isa. vii. 12), to seek to strange peoples
and their rites. Ahaz's sacrifice of his son (whvh indeed
rests on a somewhat late authority) must have been an
isolated act of despair ; human sacrifices are not among
the corruptions of the popular religion spoken of by
Isaiah and Micah. But in the 7th century, when the old
worship had sustained rude .shocks, and all religion was
transformed into servile fear (Micah vi. 1 sq. belongs to this
period ; see Micah), the example of Manasseh spread to
his people ; and Jeremiah and Ezekiel make frequent and
indignant reference to the " high places " for the sacrifice
of children by their parents which rose beneath the very
walls of the temple from the gloomy ravine of Hinnom
or Tophet^ (Jer. viL 31, xix., xxxii. 35; Ezek. xvi. 20,
xxiii. 37). It is with these sacrifices that the name of
" the Moloch " is always connected ; sometimes " the
Baal " (lord) appears as a synonym. At the same time,
the horrid ritual was so closely associated with Jehovah
worship (Ezek. xxiii. 39) that Jeremiah more than once
finds it necessary to protest that it is not of Jehovah's
institution (vii. 31, xix. 5). So too it is the idea of
sacrificing the firstborn to Jehovah that is discussed and
r^ected in Micah vi. It is indeed plain that such a
sacrifice — for we have here to do, not with human victims
in general, bui with the sacrifice of the dearest earthly
thing — could only be paid to the supreme deity ; and
Manasseh and his people never ceased to acknowledge
Jehovah as the God of Israel, though they sought to make
their worship more eflicacious by the adoption of foreign
rites. Thus the way in which Jeremiah, and after him
' In 2 Chrou. xxviii. 3 (parallc! to 2 Kings xyl. 3) a single letter is
transposed in the phrase, changing the sense from *' caused to pa.ss through
the Are " to " caused to bum with Are. " Geiger { Urschri/l uTid Ueber-
selzung, p. 305) very unnecessarily supimses that this is everywhere the
original reading, and has been changed to soften the enormity ascribed
to the ancient Hobrews. The phrase "to give one's seed to Moloch,"
Lev. XX. 2 sq., and the fact that these victims were (like other sacrifices)
regarded as food for the deity (Ezek. xvi. 20) explain and justify the
common reading.
'■' In Hosea xiii. 2 the interpretniion "they that sacrifice men" is
improbable, and 2 Kings xvii, 17 and Lev. xviii., xx. are of too late
date to prove the immolation of children to Moloch in eld Israel.
The " ban " (Diri), which was a religious execution of criminals or
enemies, w.as common to Israel with i*s heatlicn neighbours (stone of
Misha), but lacked the distinctive character of a sacrifice in which the
victim is the food of the deity, -conveyed to him through fire.
■* The etymology of the word Tophet is obscure ; its meaning
appears from lopIUeh, "pyre," Isa. xxx. "Z.
the legislation of Leviticus and the author of Kings, sceni
to mark out the Moloch or Baal as a false god, distinct
from Jehovah, is precisely parallel to the way in which
Hosea speaks of the golden calves or Baalim. In each
case the people thought themselves to bo worshijiping
Jehovah under the title of Moloch or Baal ; but thefjrophet
refuses to admit that this is so, because the worship
itself is of heathenish origin and character. " The
Moloch," in fact, like " the Baal," is not the proper name
of a deity, but a honorific title, as appears from the use of
the article with it. According to the Hebrew consonants,
it might simply be read "the king," which is a common
appellation for the supreme deity of a Semitic state or
tribe.* And so the LXX., except in 2 Kings xxiii. 10,
and perhaps Jer. xxxii. 35, actually treat the name as an
appellative ("niler," "rulers"). The traditional pronuncia-
tion, which goes back as far as the LXX. version of Kings
(MoAd^), appears to mean " the kingship " — an unsuitable
sense, which lends probability to the conjecture that the
old form was simply " the king," and that the later Jews
gave it the vowels of riC'3, the contemptuous name for
Baal (G. Hoffman in Z. f. AT.W., 1883, p. 124).
From these arguments it would appear that the rise of
Moloch worship does not imply the introduction into the
religion of Judah of an altogether new deity, but only a
heathenish development of Jehovah worship, in the familiar
fashion of religious syncretism, and under that sense of
the inadequacy of the old popular rituoJ to divert the
wrath of the Godhead which was inspired by the calamities
of the nation in the 7th century e.g., and led to more than
one new development of atoning ritual. The key to the
phenomenon is to be found in Micah vi., not in any veia
of mythological speculation as to the forces of nature, such
as is supposed in Movers's theory that Moloch represents
the fiery destructive power of the sun. Moloch, in fact,
in the Old Testament has no more to do with fire than
any other deity. The children offered to him wtre not
burned alive ; they were slain and burned like any other
holocaust (Ezek. ut siipra ; Isa. Ivii. 5) ; their blood was
shed at the sanctuary (Jer. xix. 4 ; Ps. cvi. 38). Thus
the late Rabbinical picture of the caif-headed brazen image
of Moloch witliin which children were burned alive is pure
fable, and with it falls the favourite comparison between
Moloch and the Carthaginian idol from whose brazen arms
children were rolled into an abyss of fire, and whom
Diodorus (xix. 14) naturally identifies with the child-eater
Kronos, thus leading many moderns to make Moloch the
planet Saturn. On the other hand, the JIassoretic text
of 1 Kings xi. 7 makes Moloch (without the article) the
name of the god of the Ammonites, elsewhere called
Milcom or Malcam. But in this place the LXX. translators
certainly found the longer form D37D in their MSS. (as
the Hebrew still reads in verse 33), while it is plain from
2 Kings xxiii. 10, 13 that the worship of Milcom at the
shrine set up by Solomon was distinct from the much
later Moloch worship of Tophet. In the usual printed
text of the LXX., indeed, this distinction is not made in
2 Kings xxiii. ; but this is an error of the Roman edition,
the Vatican MS. really reading MOAXOA in verse 13.
(w. E. s.)
MOLUCCAS, MoLUCCos, or Spice IstiNDs, The, com-
prise, in the wider use of the term, all the islands of the
East Indian Archipelago between Celebes on the west, the
Papuan Islands and New Guinea on the east, Timor on
the south, and the open r-nil'': on the north. They are
* Compare the Tyrian Melkart (king of the city) and the two
names compounded with vielck, "king," in 2 Kings xvii. 3i. These
latter cases are specially instnictive, because Adrommelech and Aana-
mclech were also worshipped by the sacrifice of children.
M O L — M O M
697
thus distributed over an area measuring about 450 miles
from east to west, and about 800 from north to south, and
include — (1 ) the Moluccas proper or Temate group, of which
Jilolo is the largest and Temate the capital ; (2) the Bat-
chian, Obi, and Sula groups ; ^3) the Ambon or Amboyna
group, of which Ceram (Serang) and Bum are the largest ;
(4) the Banda Islands (the spice or nutmeg islands par
txcdlence), of which Lantoir or Great Banda is the largest,
and Neira politically the most important ; (5) the south-
eastern islands, comprising Tenimber or Timor -Laut,
Larat, kc; (6) the Kei Islands and the Aru Islands, of
which the former are sometimes attached to the south-
eastern group; and (7) the south-western islands or the
Babber, Sermatta, Letti, Wetter, Roma, and Damme groups.
At the close of the 16th century this part of the archi-
pelago was divided among four rulers settled at Temate,
Tidore, Jilolo, and Batchian. The northern portion be-
longs to the Dutch residentship of Temate, the southern
portion to that of Amboyna.
The name Moluccas seems to be probably derived from
the Arabic for "king." Argensola (1609) uses the forms
idas McUucas, Maluco, and el Maluco; Coronel (1623), itloi
del Molitco ; and Camoens, Maluco.
Compare the articles on TiroiAN Archipelago, Aru Tslanbs,
Jilolo, Ternate, &c., and J. J. de Hollander, SandUiding bij
de BcoefeniTig dtr Land- en VoUxnkunde v<m Ned. Oost. Jndia^
Breda, 1877 and 1882.
MOLYBDENUM, one of the rarer metaUic elements
(symbol for atomic weight. Mo = 96; H = l), occurs in
nature chiefly in the two forms of Yellow Lead Ore
(PbOMoOj) and Molybdenite (MoSj). The latter mineral
is very similar in appearance and in mechanical properties
to graphite or black lead, and, in fact, was long confounded
with it chemically, until Scheele in 1778 and 1779 proved
their difference by showing that only the mineral now
called molybdenite yields a white earth on oxidation.
The metallic radical of the earth, after its discovery by
Hjclm, was called molybdenum, from /xoXv/SSoi, lead.
By heating molybdenite in a combustion tube in a current of air,
we obtain the trioride M0O3 (molybdic acid) as a white crystalline
lublimate. This substance, when heated to redness in close vessels,
fases without much volatilization into a yellow liquid, which, on
cooling, freezes into a crystalline radiated mass of 4"39 specific
gravity. It dissolves in 500 parts of cold, and in 960 of hot
water. It dissolves readily in aqueous ammonia or alkalies, form-
ing molybdatea. Like silica, it combines with bases in a great
variety of proportions. Of these many salts, an ammonia salt of
the composition SCNH^jjO. 7M0O3 + 4H2O (known in laboratory
parlance simply as molybdate of ammonia) is the most important,
affording, as it does, the most delicate, characteristic, and widely
applicable precipitant for ortho-phosphoric acid. To detect phos-
phoric acid in any substance soluble in water or nitric acid, add
first to a solution of molybdate of ammonia an excess of nitric acid,
and then (not too much) of the nitric solution of the phosphate,
and keep the mixture at 40° C. ; the whole of the phosphoric acid
gradually separates out in the shape of a canary-yellow crystalline
precipitate of " pkospho-molybdatc 0/ ammonia," of the composition
. 24M0O3 . PA . 3(NH4).0 I , 1 BH o
-f241IoOj. PA- 2(NH,),,Q. H3O/ +16"»"
(according to Gibbs), which is insoluble in the reagent, even in the
presence of dilute nitric acid, but soluble in excess of phosphoric acid.
By treatment of this complex ammonia salt with aqua regia we can
eliminate its acid 24Mo(33 . PA . 3H„0 as a substance soluble in
water and crystallizing from this solution with 59 molecules of
water.
This phospho- molybdic acid plays a great part in chemical toxi-
cology, being a genorically characteristic precipitant for all (organic)
alkaloids, which combine with it, pretty much as ammonia does,
into precipitates insoluble in dilute mineral acids. A solution of
the acid suiBcient for this purpose may be obtained by saturating
carbonate of soda solution with molybdic acid, adding phosphate
of soda, one part for every five of MoO^, evaporating to dryness,
fusing, dissolving in water, filtering, and addihgJnitric acid until
- the liquid becomes yellow.
Metallic molybdenum is obtained by reduction of the trioxide in
hydrogen gas at very high temperatures. It is thus obtained in
smalt crystalline granules which are infusible even in the oxy-
hydrogen flame. An alloy of the metal with four or five per cent.
IG— 2.5*
of carbon (formerly accepted as inolybdennm) fuses in the oiy-
hydrogen fiamo into a suver-white metal, of 8".6 specific gravity,
which is harder than topaz (Debray).
Analysis. — Molybdenum in all its forms is readily converted into
molybdic acid by oxidizing agents, such as nitric acid ; or if in non-
volatile forms into alkaline molybdate by fusion with carbonate
of alkali and.pitre. Alkaline molybdate is soluble in water ; the
solution, on a gradual addition of hydrochloric acid, gives first a white
precipitate, which then dissolves in the excess of acid. AVhen a
piece of zinc is added to such a solution, the latter, through
gradual reduction of its M0O3 to lower oxides, assumes first a blue,
then a green, and lastly a deep blackish-brown colour. Molybdic
acid colours the blowpipe flame yellowish green. It dissolves in
fused borax, forming a head which in the oxidizing flame becomes
yellow in the heat, hut almost colourlees on cooling ; the reducing
name colours it dark brown, and may cause the separation of brown
flakes of M0O5. Compare Chemistet, vol. v. pp. 541, 642.
MOMBASA, or less correctly Mombas, the Mmta of the
Sawahili, a town on the east coast of Africji, in 4° 4' S.
lat., with the best harbour on all the Zsjizibar mainland.
The coralline island of which it occupies the eastern
portion is 3 miles long by 2J broad, and lies in the
middle of a double inlet of the sea stretching northward
into Port Tudor (so called after the English officer who
surveyed it) and westward into Port Reitz (after the
English resident who died while exploring the Pangani
river in 1823). Except at the western end, the coast
of the island consists of cliffs from 40 to 60 feet high.
In the vicinity of the town palms, mangoes, guavaa,
baobabs, and cinnamon -trees flourish abundantly, and
farther to the west are stretches of virgin forest, the
haunt of monkeys, wild hogs, and hyaenas. The citadel,
originally constructed by Xeixas and Cabrera in 1 635,
stili remains in good condition, "a picturesque yellow
pile with long buttressed curtains," but has preserved
little of its Porttiguese architecture. Of the twenty
Portuguese chtirches which Mombasa once eontained, only
two or three can be identified. A few of the houses are
built of stone, but most of them are mere thatched huts.
The population in 1844 was, according to Dr Krapf, from
8000 to 10,000, mostly Wasawahili, but with a considerable
number of Arabs and some thirty or forty Banyans. In
1857 Burton estimated the inhabitants at 8000 to 9000,
and in 1883- they numbered about 20,000. The Arabs,
the Wamwita, and the Wakilindini (the two divisions of
the Wasawahili residents, of which the former is the original
stock) have each their own chief. In 1875-76 the Church
Missionary Society, which made Mombasa one of its stations
in 1844, established a settlement for liberated slaves at
Freretown (Kisauni) on the mainland, opposite Mombasa.
By 1881 it consisted of ab<jut 450 persons, of whom about
one-fourth were children attending school. The pupils are
taught to read both English and Sawahili {Ck.. Miss.
Intelligencer, 1875-76 and 1881). A bianch station at
Rabbai numbers 600 inhabitants.
Mombasa takes its name from Mombasa in Oman. It is men-
tioned by Ibn BaWta in 1331 as a large place, and at the time of
Vasco da Gama's visit it was the residence of Calicut Banyans and
Christians of St Thomas, and the seat of considerable comtuerce.
The "king" of the city, however, tried to entrap Da Gama, and
with this began a series of troubles which give full force to the
native name Mvrita (war). The principal incidents are the capture
and burning of the place by Almoyda (1505), Nuno da Cunha
(1529), and Duarte de Menezes (1587) — this last as a revenge for its
submission to the sultan of Constantinople — the building of the
Portuguese fort (1594), the revolt of Yusuf ibn Ahmed (1631), the
erection of the Portuguese citadel (1635), the five years' siege by the
imam of Oman (1660-65), and the final expulsion of the Portuguese
(1698). In 1823 the Mazara family, who had ruled in Mombasa
from the early part of the 18th century, placed the city under
British protection ; but Britain soon withdrew, and left the place
to be bombarded and captured by Sayyid Said of Zanzibar, who
was obUged to make repeated attacks between 1829 and 1833, and
only got possession in 1834 by treachery. A revolt against Zanzi-
bar in 1875 was put down by British assistance.
See Capt W F. W. Owen, Jiarmliw. i-c. (1833); Capt ThomM Boteler,
Karmtivt, be. (1835); OuUlain, Voyagt, (^ms, 1S56); Krapf, TmvtU, (1800) ;
Burton, Zamibar, (1S72).
XVI. — 88
698
MONACHISM
THE word Monachism, or Monastieism, primarily mean-
ing the act of " dwelling alone " (/^ovaxo?, fiovd^av,
fj-ovoi), has come, by an easy and natural transition, to
denote the corporate life of religious communities living
a life of poverty, celibacy, and obedience, under a fixed
rule of discipline. The. root-idea of monachism, in all
its varieties of age, creed, and countrj', is the same —
camdy, retirement from society in search of some ideal
of life which society cannot supply, but which is thought
attainable by abnegation of self and withdrawal from
the world. This definition applies to all the forms of
monachism which have left their mark on history, whether
amongst Brahmans, Buddhists, Jews, Christians, Moslems,
or the communistic societies of the present day, even when
theoretically anti-theological.
Thh broad general conception of monSchisra is differ-
enced ia the following ways : — It may take the form of
absolute separation, so far as practicable, from all human
intercourse, so as to give the whole life to solitary con-
templation— the anchoretic type ; or, contrariwise, it may
seek fellowship with kindred spirits in a new association
for the same common end — the ccenobitic type ; it may
abandon society as incurably corrupt, as a City of De-
struction out of which the fugitive must flee abt,olutoly —
the Oriental view, for the most part ; or it may consider
itself as having a mission to influence and regenerate
society — which has been, on the whole, and witli minor
exceptions, the Western theory of the monastic life.
The question has been warmly debated whether mona-
chism be an evil or a good, — whether a natural, perhaps
a necessary, part of Christianity (as being, indeed, t;he
strict logical issue of the triple vow of baptism, literally
construed), or a foreign element introduced into it with
unfortunate results, and rather an excrescence on its
system than an orderly and healthy development. Unlike
many other institutions which have needed the lapse of
centuries and the gradual approach of decay and degeneracy
to show their weak places, monachism in its Christian
form displays some of its most unlovely features while yet
almost in its cradle, wiereas not a few of its best achieve-
ments belong to a late period in its history ; and it has
throughout displayed a singular elasticity and power of
taking a fresh departure, after seeming to have exhausted
its energies. Its champions and its opponents have thus
alwajs had ample materials for their briefs, and there is
little probability of the controversy ever coming to an end.
But the most philosophical mode of viewing its relation to
Christianity is to recognize that monachism has made a
part of every creed which has attained a certain stage of
ethical and theosophical development ; that there is a class
of minds for which rt has always had a powerful attrac-
tion, and which can otherwise find no satisfaction ; and
consequently that Christianity, if it is to make good its
claim to be a universal religion, must provide expression
for a principle which is as deeply seated in human natm-e
as domesticity itself, albeit limited to a much smaller sec-
tion of mankind.
Driglnit- Three main factors combined to produce the phenomenon
(nfft^ of monalchism in early Christianity, each of them set in
c^uMs. niotion by the general dissolution of morals in the pagan
society of the time, of which we get a sufficient glimpse
from tlie Christian standpoint in the first chapter of the
Epistle to the Romans, and from the pagan standpoint in
the si.xth Satire of Juvenal. Tliese three factors were — (1)
the Oriental tendency towards retirement, contemplation,
and asceticism, influencing the infant Christian church
through tha agency of those Jewish ascetics, the Essenes
and Therapeutse, who had begun long before the gospel
times both the solitary and the common life in Palestine
and Egypt, and who probably contributed many converts
to Christianity, and became practically merged therein, as
they disappear from history in the iirst century of the
Christian era; (2) the Hellenic teaching of the Alexandrine
Neo-Platonists on the purification of the intellect by absten-
tion from physical indulgence ; and (3), perhaps a more
powerful influence than either, that old Roman spirit of
austerity and discipline which, while looking back regret-
fully to the memories of the simpler habits of republican
times, could find nothing amidst the social luxui-y and
administrative weakness of the decaying empire which pre-
sented its ideal, save the monastic system with its rigid
proscription of Itixury, and even of comfort, in every form.
The first-named of these three factors was, however, neces-
sarily the earliest to operate. The Scriptures attest clearly
the existence of a body of ascetics in the persons of the
Nazarites, leading always for a certajn period, and sometimes
fof life, a stricter existence than the ordinary Jew ; Elijah
and John the Baptist furnished examples of the soUtary
hermit type ; the Schools of the Prophets at least seem to
have been celibate and ccenobitic communities, living by a
fixed ascetic rule ; and it is familiar to all that such was the
actual discipline of the Essenes (see Essenes). The sect of
the Therapeutse, known to us only from the book De Fita
Co7iiemplativa (ascribed to Philo), and described as chiefly,
though not exclusively, established in Egj'pt, bore much
resemblance to the Essenes, differing from them for the
most part by greater austerity in the matter of food, and
by their preference for the solitary life over the common
fellowship of the Essenes ; for their custom was that each
member confined himself to his lonely dwelling (called by
the afterwards famous nam.e of ;iovatm]piov) throughout
the week, while all assembled on the Sabbath for joint
worship, and for instrviction from the senior of the society.
So closely does this polity resemble that of several of the
earliest Christian societies of the kind that Eusebius de-
votes a chapter of his Ecclesiastical Histm-y (ii. 17) to as-
serting their identity, holding that Philo could have been
speaking of none save Christian ascetics, a view ia which
he is followed by Sozomen and Cassian in ancient times,
as also by many moderns. This view has been rendered
much more probable by recent inquirers, who seem to
have made out that the De Vit. Cont. is spurious, and was
written about 300 a.d. ;' for there is a general agreement
amongst the fathers that the monastic life did not begin
till nearly two hundred years after Philo lived ; and Ter-
tullian (160-240 a.d.) declares explicitly that Christians
in his time did not withdraw from society, — " We are not
Indian BrAhmans or Gymnosophists, dwellers in woods,
and exiles from life ; ... we sojourn with you in the
world" (Apot., xlii.). Yet there is no reason to doubt
that the leaven of Essenism was at work in the church
from the earliest time, and helped to form the temper
which issued in monachism. Still, the jirocess was slow
and gradual, passing through very much the same stasci
as can be traced by careful inquiry in the case of the
Essenes. That is to say, the new converts to Christianity,
being for the most part dwellers in cities, were in necessary
and daily contact with the heathen society around, whose
relaxation was such as to induce i.n even greater recoil from
habits of self-indulgence than the stricter morality of their
new creed enjoined, so that a body known by the name of
" Ascetics " s|iraiig up veiy soon within the church, ami
' Sea especially Lucius, Die Thcrapcutai, 1879.
M. 0 N A Q H I S M
699
vcre urged on to still greater severity of life when the rapid
jrogress of Christianity brought large numbers of merely
lominal converts in, whose practice fell too conspicuously
jelo-.r their profession. The desire of protest against such
i state of things led to the gradual separation of the
levotees into a kind of order within the main body, .and
;o their actual withdrawa' from habitual intercourse -n-ith
;heir less strict fellows, which led in turn to their departure
■rom the towns into more secluded places, even before any
.'ormal conception of the monastic life had shaped itself in
;heir minds. But the first glimpse obtainable of the
''common life," and that only an indistinct one, is in the
STew Testament, and applies to women alone. There is
mention in the pastoral epistles (1 Tim. v. 9-12) of a class
of widows, apparently not as mere recipients of relief, but
as coiistit.Lting an ecclesiastical grade ; while in Acts ix.
39 it appears as if a number of women belonging to this
arder were united in some kind of community under the
headship of Dorcas, for the narrative rather implies that
they were her assistants in making clothing for the poor
than themselves the objects of her bounty. This conjecture
receives some confirmation from the mention of " the virgins
who are called widows " (ras rrapdevovs ras Atyo/xei'aj ^tj/dos)
in the shorter recension of the Ignatian Epistle to the
Smyrnoeans, and from the statement of Athanasius,
that Anthony, when himself about to begin the solitary
life which he is regarded as having instituted, first placed
his sister in a convent of virgins (vapOivoiva), — facts which
prove the organization of women at an earlier date in com-
munity life than of men, and lend some probability to the
notion that it may have begun very soon indeed, especially
whi?n the prominence given to the virgins as a separate and
seemingly long-established order in the church by such
early writers as Tertullian and Cyprian is borne in mind.
Two other causes must be taken into account as tend-
ing to stimulate monachism when once it began. First is
the theological opinion, early formulated, and never since
without many advocates, that two distinct standards of
life and holiness are set forth in the gospel : that of pre-
cept, and that of "counsels of perfection," — the former
binding all Christians without exception, the latter being
voluntary, and merely offered for acceptance to such as
aim at especial sanctity. The second, and even more
powerful, agent was Gnosticism, not only in its earlier
forms and in the kindred spirit of Montanism, but still
more in its lifanichcean development, when its dualism led
to exaggeration of the antagonism between flesh and spirit,
and the human body was regarded no longer as a servant
to be trained, but as an enemy to be crushed and beaten
down xvith unrelenting, hostility. But in every age of
monachism, from the earliest to the latest, social disorders
and insecurity have proved the chief feeders of the cloister,
never widely popular in times of healthy and orderly
national life, but eagerly resorted to as a place of shelter
from social turbulence.
There are five main classes of monastic institutions, each
of which approximately marks a new departure in the
history of Western monachism (for the East has never had
piore than the first), as they succeed one another in chrono-
logical order, without in any instance involving.the aban-
donment of the previous foundations. They are — (1) Monks ;
(2) Canons Regular ; (3) Military Orders ; (4) Friars ; (5)
Clerks Regular. All of these have communities of women,
either actually affiliated to them, or formed on similar
J, lines.
Early There is no doubt as to the time and the person, when,
tscetics. and by whom, the first decisive step was taken which left
a marked interval for all time between those ascetics who
continued to live in family life, if not really part of it, or who
<it least dwelt close to some oixlinary church, to which they
resorted habitually, and the seekers after some more retired
and separate mode of life, whether singly or in communities.
During the stress of the Decian persecution (249-250 A.D.)
Paul, a native of the Lower Thebaid, born of wealthy
parents about 228, was denounced by his brother-in-law
to the authorities as a Christian, and fled for safety in-
to the desert, where he established himself in a cavern,
shaded by a palm-tree, and with a spring of water close
by. There he remained till extreme old agg, dying, if
we may accept Jerome's chronology, in his hundred and
thirteenth year, about 342. Although he did not collect ■
any band of disciples around him, nor even, so far as is re-
corded, attract any casual visitors, except his more famous
successor, Ajathony, who is alleged, in a narrative con-
taining many legendary details, to have had an interview
with him when himself a very old man, the day before
Paul's death ; yet there seems reason to believe that the
fame of his example spread .suflSciently to induce imitation
of it, and that anchoretic cells began to be set up sparsely
in the deserts even before Anthony adopted that mode of
life. Anthony's career differed in various respects from
that of his precursor. In the first place, it was voluntary
choice, not fear of persecution, which sent him into solitude.
He was bom about 250 at Coma in Upper Egypt, of
wealthy Christian parents, and was left at eighteen years
of age in possession of a large fortune and of the guardian-
iship of a younger sister. He had received what was prob-
ably a fair vernacular education, but distaste for study,
or perhaps more probably that difficulty which contempla-
tive intellects experience in the acquisition of languages,
left him unacquainted with Greek or Latin ; yet the
intimate knowledge of Scripture which he aftei-wards
displayed cannot be satisfactorily accounted for in any
other way than as the result of attentive perusal, since no
mere listening to the lections in church would suffice to con-
vey it ; and we must therefore take Athanasius's statement
of his ignorance of letters to denote the absence of culture,
not as implying actual illiteracy. One day, hearing the gospel
read, " Go and sell that thou hast, and give to the poor . . .
and come, and follow Me," he took it as a direct address
to himself, and at once returned home, distributed his pro-
perty amongst his neighbours, reserving only a small sum
for the support of his sister whom he placed in charge
of some Christian virgins, and then betook himself to a
solitary life, first visiting the most eminent ascetics and
anchorets he could find, in order that he might learn the
peculiar merit of each, and imitate it. He fixed his dwell-
ing first in a tomb, then in a ruined fort near the Nile,
where he remained for twenty years, leaving it but once,
in 311, to encourage the Christians of Alexandria during
the persecution of Maximin ; and lastly in a small grove of
date-palms, a few miles west of the western coast of the
Red Sea, near the base of Mount Kolzim, where he made
an enclosure and planted it as a garden. He quitted this
retirement but once in his remaining life, when he again
visited Alexandria in 335, at the request of Athan-
asius, to preach against the Arians. Yet his fame drew
not only frequent visitors to his cell, but numerous disciples
and imitators around him, attracted not alone by his pious
austerities, but by his cheerful and courteous manners and
shrewd practical judgment. He made the soUtaiy life
honourable and popular, fully justifying Jerome's phrase
in comparing him with Paul, " Hujus vit» auctor Paulus,
illustrator etiam Antonius." When Anthony died in
365, aged one hundred and five, the desert was already
studded with hermitages in every direction, and the second
great step in the development of monachism had been long
taken by Pachomius, who stands out in liistory at once as the
founder of the coenobitic life amongst Christians and as the
author of the first formal monastic rule. Born about 292,
700
U 0 N. A. G H t S M
ana eonvcrtecl to C'hrisiianiiy in variy mantooj wnilc
jerviiig in the army, he was bajitized on obtaining his dis-
chacge, and at once adopted the ascetic life under the
direction of the hermit Palajmon; with whom he retired
to Tabenrse, an island in the Nile, between Farshoot and
Dendarah. Here he began his new institute, whose dis-
tinguishing features were as follows. The monks were
distributed into cells, each of which contained three inmates,
known in this relation as syncetli (the usual number in
other Egyptian foundations was two in each cell, while in
Syria the tenant had no partner). A large number of such
cells clustered near each other formed a laura, and each
such laura had but one common place for meals and other
assemblies. Work and food were apportioned to each
inmate according to his physical strength, and such as
were permitted exceptional strictness in fasting were not
to undertake the heavier tasks of bodily labour. Their
dress was to be a close linen tunic, with a white goatskin
by way of upper garment, which they were not to lay aside
at meals or in bed, but only when they assembled for the
eucharist, when they wore their hoods only in addition to
the tunic. They were divided into twenty-four groups or
classes numbered according to the letters of the Greek
alphabet, into which they were distributed according to
their intellectual and spiritual jtroficiency, the least intelli-
gent being placed in class i, the letter of simplest form,
and the ablest in class f, the most complicated. Each
group was subdivided into bands of ten and a hundred
under decurions and centurions, and all subject to the
Abbot, who was himself in turn, when the institution
spread and ramified, subject to the Superior (or Archi-
mandrite) of the mother-house ; while the finance of each
house was managed by a steward (oiVovo/ios), who was simi-
larly accountable to the treasurer or steward at Tabenna;.
Their usual food was bread and water ; their luxuries, oil,
salt, and a few occasional fruits or vegetables, chiefly
pulse ; frugal meals which they ate in strict silence —
sometimes broken by the voice of a reader, appointed to
recite lections fronr the Bible — each man so wearing his
hood or cowl as to hide his face from his companions.
They assembled twice daily for common prayer, and met
further for communion on Saturdays and Sundays. A
strict probation of three years was imposed on postulants
for admission, during which they were confined to simple
tasks of labour, and were not permitted to enter upon
actual study till they had satisfactorily passed through
this term. Their work was tillage for their own immediate
wants, and weaving mats or baskets for sale, to procure
such necessaries as their direct labour was insufficient to
provide ; and, as time went on, other handicrafts were
practised in the cloisters, such as those of smiths, tailors,
boat-builders, tanners, and so forth. Pachomius induced
bis sister to found a convent of nuns governed by very
.similar rules, and subject to the authority of a visitor
appointed by himself, as superior of the whole institute.
Such was the success of the Pachomian rule that before
the founder died (between 318 and 360) he had no fewer
than fourteen hundred monks in his own cccnobium, and
seven thousand altogether under his authority. Nor was
its influence confined to Tabennai and its dependencies.
Ammon carried the rule into the Nitrian desert, where
fiv6 thousand monks were soon collected ; Hilarion bore
it into SjTia and Palestine, Eustathius of Sebaste into
Armenia, Ejihraem Syros into Mesopotamia, Basil the Great
into Capiiadocia and Pontus (though a-Tulo of his own
framing sujiplantcd it later) ; and, above all, it was brought
by Athanasius himself into Italy, wlience it spread over
thj West till modified in various ways by subsequent legis-
lation, and finally displaced by the Benedictine institute.
And such v.-as its popularity, meeting as it did a need of
fhe time, that its votaries in Egj-pt alone amounted b«
the 5th ceiituryto more than a hundred thousand, of whon^
three-fourths were men. This rule has come down to \is
in two very different forma : an earlier and probably ori-^
ginal one, preserved for us in the Historia Lausiaca of
Palladius, bishop of HelenopoUs (367-430) — a great store-
house of details on Egyi>tian monachism, which is very
brief, and has been sumn'.arized above — and a muck
longer recension, extending to 194 heads or chapters, pre-
served in a translation by Jerome, in whose time thp
monks governed by it had increased to fifty thousand.
It had not, however, a complete monopoly, for there were
also similar rules in local use, going by the names of fambus
ascetics such as Paphnutius, Macarius, and Serapion ; nor
was it uncommon to find communities wherein two or three
different rules were followed simultaneously by the various
inmates. The rule of Basil, however, proved to the
East what that of Benedict did to the West, in that it
practically absorbed or supplanted all its predecessors,
while, unlike the great Western reform, it has had no subJ
sequent competitors, and remains to this day the siuglq
monastic code of the Oriental Church. This rule is
embodied in the Ascetic Sermons of Basil, and also in
two recensions, a longer and a shorter one, of the actual
provisions of his code, which are marked with not a little
of the shrewd practical sense, as well as lofty piety, which
characterized the founder, — being especially noticeable for
their discouragement of the solitary mode of life, and for
their recommendation of labour. The development of Orien-
tal monachism thus ceases with the Easilian rule, and there
are only two seeming exceptions to this fact : the institu-
tion of the Accemeti (okoi/xi;toi), or "sleepless" monk.s
in the 5th century, for thS purpose of keeping up imbroken
prayer day and night — a system copied much later in the
West by the communities founded for "perpetual adora-
tion ; " and the erection, for these very monks, of the great
monastery of the Studium at Constantinople (named from
Studius, its founder), which was the Cluny of its time and
country, as a centre of tie more intellectual monastic life,
and as the model of stateliness in ecclesiastical ceremonial.'
Greek monachi.-^m, as an institute, has no history later than
the 5th century. The monks indeed constantly appear as
factors in the controversies of the centuries which followed,
at once the polemical and the i>olitical disputes showing
them equally fierce and eager partisans (notably in tht
Iconoclastic controversy, which found them the most ardent
champions of images) ; but they cannot be said to hav<
exerted much influence upon society till a very late period
of their history, when they were instrumental in keepinj
the national spirit and the national religion alive in Russis
when suffering under the Tatar yoke, and they performed
a like service for Greece during the centuries of Turlcisl
oppression. It may further be added that, howevei
low the intellectual life of Eastern monasteries may appeal
when judged by a Western standard, the clergy who an
trained in them, technically known as the " Black clergy,'
stand much higher in character, acquirements, and general
influence than the secular or "White clergy" of the parishc.''
whether in Greece or in Russia.
It has been already mentioned that the bad Bui'e'(> irregi\iar
^ This great abbey, at the height of its prosperity, contiined more
than a llioxisaud monks, and the following list of its st^ff of office ^
hearers, due to ITieodore the Studite, may be usefnlly compared with
the Western monastic hierarchy: — 'H70t'^fi'oy {abbot), vtroTaKTm^'
(prior), otKOudfUK (treasurer), ^iriffTTj^vdpxfji (ceremouiarius), iirt-nj
prjT-^t (inspector), Kavovdpxv^ (precentor), To^tdpxTti (seneschal), kc\
Xapin}^ (cellarer), iptaryjripiot (lefectioner), ^(ffrtdptot (sacrist)
d^KTrcifTTTis (eviRilator), voffoxifios (infirmarer). One or two of th
offices do not qnito correspond in East and West, but the ef.uen]
resemblance is close.
M O N A. 0 TT T S M
70]
Wflile the system ■won the admiration of all the most emi-
nent Christian teachers of the age whicl- saw its birth and
early growth, and while we are met by a still more remark-
able fact that from the time when monachism was fairly
established till we enter on the Jliddle Ages there are
but two or three names of distinction amongst the clergy,
whether as writers or administrators, to be found outside
the ranks of monachism, amongst whom the most famous
Are Ambrose and Leo the Great, nevertheless, there is
a heavy account on the other side. Not only did the
institute speedily find itself caricatured by the Messalians,
Euchites, Gyrovagi, Sarabaites or Remoboth, Circumcel-
liones, and other companies of professed ascetics, wild in
•doctrine, vagrant in habits, and turbulent in conduct, but
the more genuine societies had scarcely fewer faults in too
many cases. Lay in their origin, and for the greater part
of their earlier history having but rarely ecclesiastics
amongst them (a single priest ordained for each monastery
to minister to its inmates being the utmost allowed for a
considerable time), they were not subject to the same strict
inspection and discipline as the clergy, in case a whole
community chose to disregard its rule ; though of course it
was easy to deal with an offender who had the tone of his
monastery against him. The clergy were subject to the
direct control of the bishops, and many disciplinary canons
of councils laid down rules for their conduct ; but this was
not the case with the monks for a considerable time — nor
i&deed ever effectively in the East — and their lay character
^ave them practical independence of any authority external
to their abbot. And, despite the stringency of the mon-
asticJrule itself, which, even before actual vows began
to be introduced (probably on the recommendation of
Basil), always involved during compliance with it the
three engagements to the observance of poverty, chastity,
and obedience, which make up the staple of the monastic
principle, and though pains were taken to exclude unfit
applicants (such as criminals, slaves who had fled for rea-
sons other than ill-treatment, or persons who had kindred
dependent on them), while a long probation was exacted
from all who were accepted, yet it was impossible that
more than a small proportion of the many thousands who
flocked in during the first enthusiasm for the new move-
ment should have had any real sympathy with the re-
straints and aspirations of such a mode of life. Severe
asceticism operates differently on different natures, and
while there are some whom it does but discipline and
refine there are more whom it tasds to eoarwn aa.-i to
brutalize, even apart from the many whom it is apt to
afl'ect with morbidness, if not actual insanity. And it is
unquestionable that vast numbers of those who entered
on the monastic life came from the poorer classes, in
search of some less toilsome mode of existence than they
had previously led, preferring the contemplative societies,
■wherein almost no labour, certainly none of a severe and
trying cast, was practised, to those where agriculture and
•other active employments, requiring more energy than mat
and basket weaving, were enjoined. Such men, unedu-
cated and undisciplined, ■were liable to be thrown entirely
out of gear by the complete revolution in their mode of
life, — especially when the community they joined was not
only contemplative, but situated in some place where the
ungrateful soil made tillage nearly impracticable, and the
vast numbers crowded together were far too numerous for
any tasks which could be assigned them. From the bosom
of such societies came not only single examples of exagger-
•ated spiritual pride, bitter fanaticism, avaricious greed of
the scanty articles whose usufruct was permitted, fierce
sensuality,- and wild religious delusions, but they gave
birth to companies like the pcxrKot, or " grazing monks,"
cf , Mesopotamia and Pa'estine, who roved about, shelter-
less and nearly naked, as Sozomen and Evagriu.* tell us, in
the mountains and deserts*, grovelling on the earth, and
browsing like cattle on the herbs they casually found ; and
to those fierce bands of Nitrian and Syrian ascetics who,
reared in the narrowest of schools, treated any divergence
from their own standard of opinion as a crime which they
were entitled to punish in their own riotous fashion, two
instances of which have left an indelible brand on their
history — the murder of Hypatia in Alexandria, and that Oi
the patriarch Flavian at the Eobber Synod of Ephesus. An
equally singular, but more sporadic and temporary, fonn
of asceticism ■nas that of the Stylites or Pillar-hei'mits
(oTvA.tTot, KioviToi), who foUowed a fashion first set by
Simeon, a Syrian monk who spent almost half of the 5tl»
century on the summit of a colmnn 60 feet in height.
This unwonted kind of au.^tei ity at first gave rise to strong
objections, even from hermits themselves, and a messenger
was sent to Simeon, bidding him in the name of a synod
of bishops to descend from his pillar, but with instruc-
tions to permit him to remain if he showed himself ready
to comply. Such proved to be the case; and, having thus
assured themselves that he ^\as not influenced by spiritual
pride, they left him to follow his own devices. And we
have the direct personal testimony of the wise and tem-
perate Theodoret that h? exercised a strong and salutary
influence over the nomadic Saracen tiibes, converting many
hundreds and even thousands to Christianity, besides being
the shrewd and trusted adviser, not only of the peasants
who flocked to him for coimsel, but of Arab princes, Per-
sian kings, and even Eoman emperors. He cannot be
judged, therefore, by ordinary standards, and it is more
than likely that a less extraordinary mode of life would
have given him less power for good ; but he is the only
eminent figvire in the class to which he belongs, and the
fashion he set may be said to have died out with his name-
sake, the younger Simeon, a century later. Even when
the healthier side of monachism as it appeared in Egypt
and Syria is dwelt upon, and the fullest weight is allowed
to the contemporary pictures drawn by great Christian
writers of the monasteries as schools of a philosophy truer
and purer than that of the Porch or the Academy, as
places where the equality and brotherhood, merely dreamed
of as-vmrealizable fancies in the outer world, could be seen in
living action — where children, deserted by their parents or
other^wise orphaned, ■n-ere carefully reared — where the sick
were lovingly tended — where calmness, piety, and self-for-
getfulness were the rule of all, — it must be confessed that
the complaint of the Government, embodied in the hostile
legislation of the emperor Valens in 373, subjecting
monks to the conscription (which drew forth an indignant
protest from Chrysostom), that monachism was injurious
to society and to the healthy condition of civil life by
draining off so large a fraction of the population into tht
backwater of the cloister, was perfectly well founded.
And no small part of the overthrow of Christianity in
Egypt and Syria by Islam is due to the practical with
drawal of all the devout from family and public life, leaving
no spiritual energy to cope ■with the Koran in the towns
and villages whither the conquering Arabs came to settle
and proselytize.
The history of monachism in the West is far more varied, Pi-opajn«
chequered, and interesting than in the East. It takes •j"'^;"
its beginning from the visit of Athanasius to Home in "' " •
340, during his second term of exile, when he brought
with him his Life of St Anthony, and pressed his example
on the Roman Christians who mourned as patriots, not less
than as devotees, over the lax and enervated habits of
society. The popular imagination was caught at once,
and not only was the basis of monachism successfully laid
in Rome itself, but Eusebius of Vercslli introduced it
-02
M 0 N A C H I S M
into northern Italy, where it was' fostered a little later
by the illustrious An-?-rose at Milan, v From the very
bei^iiming a marked dih'erence shows itself in the spirit of
Western monachism as compared with the parent institute
in the East. Parfh" from dissimilarity of climate, but still
inrre from that of racial and national temperament, there
has always been less tendency in the West to either abstract
contemplation or severe self-torture, such as is equally
common to many of the Eg)'i3tian or Syrian ascetics and
to the Jogis of Hindustan. Hard work, with due inter-
vals far food and recreation, occupied all that part of a
Western monk's time which was not devoted to prayer or
study, and a careful apportionment of his duties through-
out the day gave each hour its appointed task to be ful-
filled, leaving very few loose ends of time to be wasted.
It is true that the Basilian rule aimed at this same end,
and that a very minute time-table forms a part of other
early Eastern codes ; but, as already remarked, the work
was neither hard enough nor abundant enough to provide
rjally healthy labour, or to occupy tbe mind sufficiently
to keep it from vague speculation or morbid brooding dur-
ing the hours of so-called toil.' From this fundamental
unlikeness springs the broad distinction between the two
types of the monastic life, in that the West did not merely
provide shelter for such as felt unable to endure the storms
of the world, leaving secular society to take care of itself
as best it could, but, contrariwise, employed the cloister
far more as a training-school for the strong, as the stand-
point whence to work the lever which moved a world.
Even the more remotely secluded monasteries of the West,
instead of serving as refuges wherein the inmates might
effectually cut thems'elves^ off from all iutercourse from
without, were rather military outposts and frontier forts
of eiviUzation, which taught the, arts of peace, the pro-
cesses of agriculture, and at least 'the rudiments of social
morality,' to^ the rude- and ^almost nomadic hunters and
forayers, of whom many of the wilder tribes in outlj-ing
districts consisted. And if such was the case even where
the conditions seemed least favourable, it may readily be
understood what an ample field for exertion the more
settled regions provided.-'
It would seem that it was some modmcation of the
Pacjiomian rule , which f.rst made its way into Europe,
but the interest excited by the movement led to variety
of choice on the part of tho teachers who aimed at spreading
its influence in Italy. Thus, Urseus, abbot of Pinetum
(probably near Ravenna), translated the Basilian rule into
Latin, and it soon took root in southern Italy, where it
'continued to hold its ground for a considerable time.
But a far more important part in the propagation of the
monastic institute in the West was taken by Jerome, who,
after spending a considerable time, beginning in 374,4
first as % hermit in the desert of jChalcis, and later at
Constantinople, returned to Rome in 382, where ho
was secretary to Pope Damasus. He acquired much
influence over a distinguished group of Roman ladies of
hi"h social po'sition, the most celebrated of whom are
Paula, and her daughters Blesilla and Eustochium, and
employed that influence in urging the adoption of the
monastic life upon them. Blesilla died early, it ^vas said
and believed in consequence of austerities pressed upon
her which her constitution was unable to bear; and the
unpopularity which this report brought upon Jerome,
co-operating with the death of his patron Damasus and
other causes, drove him. bade to the East, whitlier Paula
and Eustochium also betook themselves, finally settling
down in Bethlehem, vrhevi the elder lady built three con-
vents, of one of which she was superior, while Jerome, who
similarly erected a monastery for monks in tho immediate
vicinity, acted as chaplain and director to tho community.
As the taste for pilgrimages had already become«diep!y
rooted, the convent at Bethlehem was ere long a favourite
resort of pilgrims, and exerted considerable influence in
prompting the erection, of similar foundations in the
West. Quite another impulse was given to the further-
ance of monachism by Augustine. While, amongst the
many documents which have been ascribed to him, the only
one which is of the nature of a monastic code is his 109th
Epistle, addressed in terms of severe reproval to the nuns
of a convent he had himself founded at Hippo, but which
had fallen away from discipline, his personal example
gave rise to a new type of the common life, in that he
formed a sort of college of priests, who shared the episcopal
house with him, ate at a comijion table, and copied in
other particulars the observances of monasterie* but with-
out losing their secular character. This was the origin of
the institute afterwards famous as the Austin Canons, 'a
foundation of the 11th century.-' It is true that Eusehius
of Yercelli had anticipated Augustine by collecting the
clergy of his cathedral (and, as it would seem, tiie remain-"
ing ecclesiastics of the city) into a common dwelling, but
the difference in his case was that he obliged them to adopt
the habit and style of monks, and thus was in no sense the
originator of a new institute. Another important contri-
bution of Augustine's to the history of the common life is
his treatise Se Opere Mo7iachoruin, wherein he sets forth the
imperative need of making hard work an invariable factor
of the monastic profession, notably on the ground that
most of the monks in Africa came from the lower ranks .
of society, such as freedmen, farm-labourers, and artisans,
who were spiritually injured by being raised into a grade
viewed witli more 'general respect than that from which
they had sprung, while they were actually subject to fswer
privations and lighter employment than they had been
accustomed to. And he adds that amongst other "evil
consequences of this idleness was that they were found
tramping the country selling sham relics, which they
palmed off on the unwary, extorting money in other
fashions also, and bringing discredit on their profession
by their hypocrisy and vices — a picture only too faith-
fully repeated by the Mendicants a thousand years after
the date of this treatise. The 5th century was one of
rapid progress in the spread of monachism in the Vrest.
Chief amongst those who heli>ed to popularize it stands
the name of John Cassian (3-50-433), a monk of Bethlehem,
who made a long and careful study of the Egyptian
forms -of monacliism, of which he has bequeathed us valu-
able details in his De Insiitiitione Ccenobioniin and Col-
laiiones Patrum, tho former of which is a treatise on the
monastic life, and indeed virtually a rule, though a som.e-
what prolix one, mainly derived from Macarius, while the
latter is a record of the teachings of some hermits of the
desert of Scete. ' Both of these works exercised a powerful
influence in their o%\'n day, and the second retained its
repute much longer, having been warmly approved and
recommended for study by Benedict, Bruno,' Dominic,
and Ignatius Loyola, all four founders of celclirated orders.
Cassian fixed himself at Marseilles, whete he founded a
famous monastery of. which he was probably abbot, and
which was the centre -H-hence monachi.^m, uniting the
peculiarities of East and West, was jiropagated in southern
Gaul, and notably planted in the island of Leriiis,
which became the seat o£ one of the most em;"<'nt
monasteries of the early Jliddle Ages. Northern Gaul
had received the institute earlier through .the agency
of Martin, bishop of Tours (3IG-397), who founded
monasteries near Poitiers and in his own diocese, which
were soon thronged, so that his funeral was attended b;
two thousand monjcs. Spain was even earlier in the fielc
than Gaul, but there is some obscurity as to the_historj
Tvl 0 N A 0 H I S M
703
of the introduction of mciacliis.ci there, aU that is certain
being that it had made its footing good before 380, the
date of a council of Saragossa (Caesaraugusfa) which for-
bade priests to assume the monkish habit. Still more
obscurity hangs over the first establishment of monachism
in Britain, as to which no trustworthy records have come
down to us, though all probability points to its importation
from Gaul in some variety of the Pachomian rule ; while
Germany did not receive the institute till tha following
centuj-y.
It must not be supposed, however, that the principle of
monachism met with no opposition in the course of its
progress. Apart from the opposition of those who disliked
it precisely for its merits, for its protest against the
dissolute morals and enervated habits of a luxurious and
rotting society, and for the manner in which it won to
itself many of the noblest and most promising of the
young and ardent of both sexes, and without taking into
account the more reasonable objections of statesmen, there
were not lacking warnings of the dangers attending
exaggerations of the principle of monachism, uttered by
some of its most eminent upholders. Augustine's sharp
censures have been already mentioned, and to them may
be added the decrees of the council of Gangra in 363,
or thereabouts, which anathematize those who adopt a
celibate life on the ground that marriage is evil, who wear
a peculiar dress as a mark of holiness, condemning such
as use ordinary clothing, or who desert their parents or
children dependent on them under the plea of desiring to
lead an ascetic life. So, too, the great Chrysostom, him-
self a warm advocate of monachism, found himself obliged
to teach his flock the sanctity of Christian family life, and
the truth that there was often as much selfishness as piety
in retirement to a hermitage from the cares and duties of
society. • These arguments and decisions were, however,
aimed only at abuses and exaggerations of the monastic
idea. It remained for Jovinian and Vigilantius to assail the
actual principle. Their writings have not survived, and
we can judge of their arguments only from the account
given of them by their chief opponent Jerome, whose
eminent gifts, however, did not include either moderation
or controversial fairness, so that it is not safe to assume
that we have all their case before us. As regards
,Vigilantiu3, he accurately represents the Puritan type of
mind protesting against the external part of the popular
religion of his day, often with good reason, but also show-
ing equal intolerance for harmless, if not useful, practices ;
so that his condemnation of monachism is only part of his
general objection to the temper of his time. But Jovinian's
objections seem to have gone deeper. He had been him-
self a monk (and indeed never resumed secular life), but
he disputed absolutely the thesis that any merit lay in
monachism, celibacy, fasting, and asceticism considered in
themselves, save in so far as they contributed to foster the
Christian temper and life, which might and did flourish
equally, he urged, under quite different conditions, whue
it was by no means unfrequent for spiritual pride, if not
Manichaean error, to lay hold of those who devoted them-
selves to the ascetic profession. This was, in fact, going
very little further than Chrysostom had done, or than
Xilus did a short time later. But Jovinian's divergence
from the standard of his day was not confined to practical
questions ; it extended to theological doctrines also, and
jw;cor.dingly his strictures on monachism, probably more
incisive and less qualified than those of its other critics,
were involved in his condemnation as a heretic by synods
at Rome and Milan in 390. The reaction, of which he
may be regarded as the mouthpiece rather than as the
sole representative, was thus effectually crushed, and that
for centuries. And though Jovinian is undoubtedly more
in accord than his opponents with the modem temper on
the subject of monachism, and while it may be allowed
that his teaching might have been a useful corrective in
Eastern Christendom, where family Ufe was all but over-
borne by asceticism, yet the impartial historian must
admit that his success would have been an irreparable
misfortune for civilization in the West. Such a dispas-
sionate estimate of asceticism asjiis, if widely entertained,
would have been fatal to the spread of monachism, and
thus one of the most important conservative and statical
forces in the preservation of the older culture, one of the
most powerful dynamical forces in reducing the chaotic
materials of early mediaeval society to order and coherence,
would have been lost to Europe; nor is it easy to conjecture
what effectual substitute could have taken its place. As
it was, the movement was not checked for a moment by
this partial reaction ; and not only did the older com-
munities thrive and spread during the 5th and early 6th
centuries, but new ones were established, — chief among
which stand those of Csesarius of Aries and of Donatus
of Besan^ou in southern Gaul, that of Isidore of Seville
in Spain, and the early Celtic code, of which only tradi-
tional fragments survive, but which seems in Britain to
have been strongly affected by tribal influences, so that
a monastery was often recruited from a single clan, and
the abbacy became hereditary in the family of the chief-
tain, a fact which is noticeable even in the succession of
the abbots of lona, who for ten elections after Columba
were of his. family in the tribe of Conall Gulban.^
But, swiftly as monachism spread in Europe during the
breaking-up of the Western empire, some of the causes
which hastened its progress also tended to its rapid de-
cay. The disturbed state of society, and, in particular, the
prevalence of petty warfare, drove many thousands of
persons to seek a quiet refuge in the cloister without any
more directly religious motive. When once there, they
found in every place some rule in force which was either
imported directly from Egypt or Syria, or else, like that
of Caesarius, modelled on Eastern lines, and therefore
ill suited to the severer climate of Europe and the more
active habits of the people. The austerities were thus too
oppressive for general observance, and the result was a
widespread neglect of nilea which continued nominally in
force, while at the same time the very monks who had
ceased to keep them laid claim to special sanctity on the
pretence of their strict way of life. The time was ripe
for a reform, or rather for a wholly new departure in
the shape of a rule devised to meet Western needs, and
not merely adapted more or less clumsily from Oriental
asceticism. The fitting man to accomplish this difilcult
task appeared in the person of Benedict of Nursia, author
of the most famoxis of all monastic codes. Bom of a
respectable family about 480, he adopted the ascetic life
at fourteen in a cave near Subiaco, not far from Rome,
where he remained for three years, at the expiration
of which he was chosen abbot of a neighbouring con-
vent, then in a very relaxed state. His rule proved
too stem for his new subjects, who attempted to poison
him, whereupon he resigned his office and returned
to Subiaco, around which he soon erected twelve monas-
teries, each peopled by an abbot and twelve monks.
Fresh attempts on his life and on the discipline of his
society drove him out again in the year 528, when he fixed
his dwelling at Monte Cassino, the place where his cele-
brated rule was drafted in the following year, and which
has ever since prided itself on its rank as the cradle of the
Benedictine Order and the premier abbey of Western
Christendom. The famous institute which he devibcd
' AdamDan, T'l't Columb., ed. Reeves.
704
Rule ot
Bene*
diet.
has a great surface likeness to the rule of Basil, which
alone has rivalled it in permanence, though far below it
m diffusion and, it may be added, in services to humanity
Superior in flexibility and in the power of adapting itself
Vn new conditions of circumstance and society to any rule
which preceded it (and indeed to most of those devised
later), the effect it produced in its own immediafe day and
for several centuries afterwards is almost incalculable
„iv>, ■?"• ""I™"', ^""'"'ty: worship, study, and work; such
are the ideas and employments with which this code of seventy- three
chapters is occupied. It opens with a sermonet or hortatory preface
and then proceeds to define the e.^sting classes of monks, as divided
into Ccenobites, Anchorets, Sarabaites, living by twos and threes
together without any fixed rule or lawful superior, and Gyrovari
vagrant tramps y,ho, even at that time, as more than a century
earlier, continued to bring discredit on the monastic profession It
was one great aifn of the Benedictine reform to extirpate these Uvo
latter classes, and the method adopted was the addition of a fourth
vow, that of " subility," to the three usual pledges. This fourth
vow bound the monk to continuance in his profession, and even to
residence for life at the monastery in which he was professed, unless
temporary absence or permanent transfer were permitted by the
authonties and thus struck directly against the temper of restless-
. nes3 and desue for change which were such powerful factors in
generating the irregular and wandering classes just named. Chapter
11. describes the nualities of an abbot, and also decrees that no dis-
tinctions of worldly rank or station are to be recognized amonc^st
the imnates of the monastery. Chapter iii. is one of those whi^h
best enable us to estimate the foresight and good sense of Bene-
dict It enacts that the abbot is to call the entire bodv of the
Z.^Y'1 l°ffl l' '\<J'="^'-tt^ on any weighty matter, and not to
decide It tllT he has heard the counsel of even the very youngest ;
while m matters of less moment consultation with the elder members
suttees Chapter iv. enumerates the instruments of good works
summed up in seventy-two pithy maxims, mainly SoriptSral in letter
or spuit Chapter v. is on the obecUence of disciples. Chapter vi
13 on siJence, recommending spareness and wholesomeness of speech'
but not laying down any hard-and-fast rules such as those of the
Trappists of a later day. Chapter vii, treats of humility, includin-
JS''""^u'Tl '"/'"' T}'^ '" ""f'^^s his secret faults and thoughts tS
the abbot, to do nothing but what the common rule or the examole
of his seniors teaches, and to exhibit lowliness and meekness in out-
ward beanng as well as in the inward spirit, Chaptei-s U.-xx. are
occupied with directions about the performance of Divine service
so far as relates to the recitation of the Canonical Hours, seven of
day and one of the night. Chapter xxi. provides for the
appointment of deans (officers over ten monks) in large monasteries
to be chosen by merit, and not by mere seniority. Chapter xxii
prescribes rules for the dormitory, each monk to have a separat^
bed with suitable coverings, and to sleep in his habit, and ^irded
50 as to be ready to rise at a moments notice, and a light is to be
kept burning; m the dormitory till morning. Eight chapters (xxiii. -
X.X.X.) then deal with offenders, a graduated scale of penalties being
provided: first private admonition; next, separation from thi
brethren at meals and recreation ; then scourging; and, finally ex-
pulsion m the case of hardened olTenders, but not until the abbot
has used every means to soften and reclaim them. Even in this last
event the outcast may be received again, and that thrice, on the
T.„ aV .;? fi^"? his seniority and descending to the lowest
place. After the thud expulsion, return was finally barred. Chapter
Jjxx. ,s on the character and duties of the cellarer, an imporL[
oltcer in monasteries ; who was steward, and had the charge of all
the stores, and the responsibility of serving them out as needed j
while the next chapter provides for the appointment of inferior
?„„ mM»^' ''1"""° "l'^' '°°''' '^'"^''- ™'l "ther goods belong-
i^£l» „ monastery Chapter xxxiii. prohibits any monk to giv?,
receive, or keep aught as his o^vn without leave of the abbot whi
IS however, bound to supply him with all necessaries. Murm'urin"
at anything in the manner of distiibution is censured in the nen
chapter as a very grave offence. Chapter x..xv. ordains that the
reason of sickness or some more unportant occupation, and that who-
ever IS on duty on Saturday is to clean up for the week and tn
deliver all the cloths and utensils to the cellarer i . good clntdition
for his successor in office. Chapter xxxvi. . while warnin- the s ck
not to be impatient or exacting, gives careful direotions°for their
CO nfort They are to be placed in an infirmary and to be com-
mitted to the care of a competent attendant, are to be allowed baths
.-la olten as is expedient, and a flesh diet to promote their recovery
though agsinst the rule for those in health. Old men and children
are also to bo dispensed from the rigour of the rule, and they may
have their meals before the usual hours, instead of waiting for the
others. Chapter xxxviii. directs that reading aloud duiin- meals
M to be practised, and that no conversation, even about the°subiect
of the reading, is to be carried ou by the brotUrgu who are to keen
M O N A 0 H I S M
It- I aT^ "^1 '^ '^'y """^ anything. The reader is to be
appointed for a week and to enter upon his duties on Sunday He
IS to be allowed a ittle food before heldnning his task, lest he should
become famt, and is to finish bis meal afterwards along with the
kitcheners and waiters. And the readers are not to t.4e turns of
auty ui order, but only such persons are to be appointed as can dis-
charge the office satisfactorily. Chapters .x.xxix. and xl prescribe the
tftU^'Tfr"^ r^■^'°'^■ ^™ ""^^^ ^^^ UlowXcon"4ng
ol t^^o cooked d^hes ipubuclaria), to permit a choice of food, lest
one or other dish should be unsuitable to any one, and a third dish
ot truit or youn- vegetables is granted as an occasional addition
A pound of bread IS to be served out daily for each, though the abbot
IS empowered to increase the rations of such as had extra hard work
to do; while the rations of children are to bo proportionably
dmiin.shed and flesh-meat is forbidden to aU except tfie sick and
weak, but there is no prohibition of any flesh save that of four-footed
beasts, thus leavmg the use of poultry, eggs, and fish optional
One pint of wine daily is allowed to each monk, but the hesitation
r,;,^ '''^'J*^}^ '^ conceded is noteworthy ; and, while the prior is
empowered to increase the allowance if he judge it well, the brethren
are told that voluntary abstinence is the best course, and that where
a house IS too poor to brovide wine those debarred from it are not
to murmur Chapter xli prescribes the hours for meals at different
bv davlilt 1^1"%'"' ^V",« ^^^^ '^^^ '"'"' "«als shaU be taken
by daj h^ht, without need of lamps. Chapter xlii. directs the monks
of ra,<Z f"ll ri"""« "^"r ^ ''^^^- P'-^f^'-ably of the CoUatu>,u
of Cassian, followed by compline, after wtich silence is to be strictly
observed, save for some necessary cause. Chaptei-s xliii.-xlvi im-
pose penalties for mijior breaches of rule, such as coming late to
prayers or meals. Chapter xlvu. gives some further directions as
to Divine service, throwing on the abbot or his deputy the responsi-
baity of notifying the hour for it, ard provides thlt no incompetent
person shaU be set to chant or read. Chapter xlviii., although
brief, ,s one of the most important and characteristic in the rule
It IS on daily manual labour, and begins with the pithy axiom'
Idleness is an enemy of the soul" (Otiositas inimimcstanimm)
It proceeds to enjoin that the brethren are to distribute the time
not already taken up ^v,th prayer, meals, and sleep, into periods of
manual labour or devout reading. From Easter till the 1st October
they are to work from prime till the fourth hour. From the fourth
tilT^fZ :'" '•' ^'v ^'"' }^'y ^" *° '•"'^' On rising from meal-
time alter the sixth hour they are to rest in silence on their beds—
the lamUiar ««ta of warm countries— but those who prefer to read
may do so, provided they disturb no one. Nones are to be s2d
about the middle of the eighth hour (2,30 p.m.), and then work U
to be resumed till evening. From the 1st October till the heginuinc
»L •'^T'''' ^ ';,?\ «'l.the second hour, then to saf terce"
after which to work till the ninth hour. At the ninth hoLr they
are to leave off work, and after their meal to read spiritual books or
the Psalms. In Lent they are to read from the morning tUl the
third hour, then to work till the end of the tenth hour. And every
rfLZi° Yr \ '■ f'^l" ?"' '° '""^ ''™" *!"' 'i''™>-y at the be-
ginning of Lent, which he is to read through ; whUe tivo senior
brethren are to go the rounds during reading hours to see that tie
monks are actually reading, and neither lounging nor gossiping
On Sunda)^ all are to read throughout the day, except sucl as^"fe
special duties to discharge ; and Tf there be any who either cannot
or will not read or meditate, some task to keep them from idling is
to be assigned them. Sickly and delicate brethren are to be rifeu
light work, suitable to their health. Chapter xlix. suggests, t-ilh-
out commanding, the adoption of some voluntary self-dl^al durine
Lent, to be undertaken with the abbot's approval only, -austerities
without such sanction being denounced as vainglorious. Chapter
1, directs that brethren who work at a distance, so as to be unable
to attend common prayer, are to recite the oflice where they may
happen to be. Chapter li. prescribes that monks sent on an errand
and expecting to return the same day, are not to eat while out'
unless they have special leave from the abbot. Chapter Hi. rives a
few directions as to behaviour in the oratory. Chapter liii. contains
rules for the entertainment of guests. The most noteworthy pro-
visions are that the abbot is licensed to break his fast with th.
guests unless on a church fast-day, in order to bear them company
at meal-tunes ; that the kitchen for the abbot and guests is to be
separate from the general kitchen, and served by the s.-.mo two
brethren for a year, to insure that no additional labour may fall on
the ordinary kitcheners through the une.x]iected arrivals of strangers
needing to be fed ; that the guest-room be entrusted to a brother
(the hospitaller), and that no monk shall speak to or mix with the
fn'vi!'™'";-^^ ''y.'P^f'"' appointmcnt-a very salutary regulation,
»n, ,h u ""> ?;'««"a>>eous rout of visitors lilely to apply for food
and shelter Chapter l.v. forbids monks to receiVe letters, tokens,
or gifts, even from their nearest kin, without the abbots permis:
sion, or to give any such things to another ; and the abbot is em-''
powered to transfor>rcsents to some person other thnn him for whom'
fi „., „. .-■-■— -i"'-^;-"" lu »onio person otiier thnn him lor whom'
nZZr '"'""'''•^ .Chapter Iv. prescribes the dress, and, with'
Benedic a usual good sense, leaves it wholly in the abbot's dis-'
cretion to provide clothing suitable to the climate and Uocalily
MDNAC.HISM
705
merely ruling that in temperate pUcea a cowl and tunic, thick in
winter and tUin in aummer, with a scapular (a sleeveless woollen
uarment passed over the head, and falling down over the breast and
5ack) for work hours, as also shoes and stockings, all of the ordinary
<'ountry make and cheapest kind, shall suffice. Each monk is to
have a change of these garments, to allow of washing, and yet
another for use when sent on a journey, to be of rather better
materials, and to be kept in the general wardrobe when not in actual
wear. The old clothes are to be given up when new ones are served
out, and are to be laid by in the wardrobe for the poor. A straw
mattress, blanket, quilt, and pillow are to bo furnished for each
bed ; and in addition the abbot is to give every monk a knife, a
pen, a needle, a handkerchief, and tablets. Chapter Ivi rules that
the abbot is to take his meals with the guests and strangers, with
the privilege, if guests be few, of inviting any of the brethren he
•chooses, so long as some seniors are left in charge. Chapter Ivii.
prescribes that craftsmen amongst the brethren are to work with the
abbot's permission, and if their work is to be for sale, those who are
entrusted with making the bargains are to deal honestly with pur-
chasers, and to sell rather below the'current trade price. Chapter
IviiL lays down the rules for the admission of new members. It is
not to be made too easy. The postulant is to be allowed to knock
for entrance in vain for four or five days, then to be brought into
the guest-room for a few days more, and so be transferred to the
novice-bouse,' where he is to remain under the charge of a senior
monk for two months. If he persevere at the end of this time, the
rule is to be read over to him, and the option of departing or remain-
ing is to be offered. If he persevere, he is returned to the novice-
house for six months' further probation, after which the rule is again
read to him as before, and yet a third time after a further term of
four months. Not till he has surmounted this final ordeal can he
be admitted into the community, and before that is done he must
divest himself of his property, either giving it to the poor, or mak-
ing a deed of gift to the monastery. Then he is allowed to sign the
act of profession, including the vow of stability, which he is to lay
with his own hand on the altar. Chapter lii. provides for the
<ledication of young children, noble or poor, by their parents to the
monastic life, and requires a promise from the latter never to endow
the oblate with any property, directly or in trust, though they
-may give to the monastery if they please and reserve the life-income
to themselves. Chapter Ix. regulates the position of pnests who
desire to live in the monastery. They are to enjoy no relaxations
or priority in virtue of their ecclesiastical rank, though the abbot
may assign clerical functions to them ; and a somewhat like rule is
laid down for clerks in minor orders. Chapter Ixi. provides- for the
reception of sti-ange monks as guests, and for their admis.sion if desir-
ing t« join the community. The abbot is enjoined to listen to any
criticisms such a guest may offer, and is empowered to give him, if
accepted as a new member, higher standing than that of his entrance,
but is forbidden so to admit a monk of any known monastery with-
out the consent or letters commendatory of its abbot. Chapter Ixii.
rales that the abbot may choose a monk for ordination as priest or
deacon ; but the ordineo is to rank in the house from the date of his
admission, except when officiating, or if the community and the
abbot single him out for promotion by merit. If he misbehave, he
is to be reported to the bishop, and if continuing to misconduct
himself, sliall be exiielled, — only, however, in case of obstinate dis-
obedience to the rule. Cliapter Ixiii. lays clown rules for the gradation
of rank in the community, an<l warns the abbot against arbitrary
government. Cliapter Ixiv. allows the abbot to be chosen either by
the common consent of the whole community, or by a select electoral
committee ; and tlie lowest in standing may be chosen, if fit. In
tlie event of a bad choice, the bisliop of the iHocese, the neighbour-
ing abbots, or even tlie neighbouring laity, if having reason to think
the electioiv made .for the purpose of keeping up abuses, may annul
it and appoint another superior. Chapter Ixv. sneaks of the niis-
i-hief occasioned in many monasteries by the rivalry of the provost
or prior with the abbot, and advises that no such oflficer be apjiointed ;
yet, if the circumstances of the place need one, the abbot may name
a brother to the post, but he is to be as entirely subject to the abbot
as any other monk, and may be admonished, deposed, or exitelled
for misconduct. Chapter Ixvi. directs the apiiointment of a porter
to answer at the gate, and further recommends that every iiouse
shall have its own well, mill, garden, bakery, and handicraftsmen,
to avoid the need of intercourse with the outer world. Chapter Ixvii.
directs that llo muik shall quit the cloister without leave of the
abbot, and that, on the return of any from a jouniey, tliey are to beg
the prayers of tlie community for any faults they have committed
diirtlig their absence, and arc forbidden to speak of what tiiey have
li.ard or seen outside. Chapter Ixviii. bids a monk who has received
a hard or imiwasible command to undertake it patiently and obedi-
ently. ■ if he find it beyond his jiowcrs, lie may mention the cause
quietly to his superior ; and, if the command is srifl persisted in, he
iiiu.-it obey as bc-^t he can. Chapter Ixix. forbids monks to upliold
or defend one another in the monastery, even their nearest of kin.
Chaptei Ixx. forbids striking or excommunicating another, witliout
.■•.he abbot's authority, and j>rorides that children, until fifteen, shall
be subject to discipline &om all the monks ; but any who shall
chastise those above fifteen without the abbot's leave, oi be unduly
severe towards the younger, shall be himself puuiahable by rule.
Chapter IxxL lays down that the principle of obedience is to prevail
throughout the community, not only towards the abbot, or his
officers, but from the juniors towards their seniors. Chapter Ixxii
is a brief exhortation to zeal ; and chapter Ixxiii. a note to the effect
that the Benedictine rule is not offered as an ideal of perfection, oi
even as equal to the teachings of Cassian and Basil, but for mere be*
ginners in the spiritual life, who may thence proceed further.
It has been necessary to make this detailed analysis of
the rule, because no mere summary of its general scope
conveys an adequate notion of it ; and it plays so import-
ant a part in the history of European civilization that it
is expedient to obtain a clear idea of its details as well as
of its main outlines. The first pecviliarity in it meriting
attention is the absence of any severe austerities. Plain
and bare as the food and lodging appear if tested bji
modern notions, yet it is to be remembered that what ia
called " comfort " is a wholly recent idea, and even stUI
scarcely familiar, it may almost be said, out of Great
Britain and its colonies. The scale of -living appointed by
the rule secures a greater abundance of the necessaries of
life, not only than was at all common amongst the Italian
poor of the 6th century, but than is to be found amongst
the humbler peasantry of any European country at the
present day ; while even the excluded superfluities entered
but little into the habits of any save the very wealthy.
Next, high thinking — the highest thought of the time-
was united with this plain living, as the considerable stress
laid upon reading attests. To this part of the code is due
the great service performed by the Benedictines, both in
the erection of schools, and in the preservation of almost
all the remains of ancient Latin literature which have
come down to us. It made it not only possible but easy
for them to become a learned order, and it is a verf:
imperfect estimate of the stride fqrward in this provision
which Milman makes, when he views the injunctions as to
reading in the mere light of expedients to fill up time
somehow. If it were so, the hours for reading, would
have been fewer, shorter, and more occasional, merely
rounding off the intervals between times of labour; but they
are just as prominent and nearly as long as these. It ia
true that Benedict, whose own education had been abruptly-
broken off by his early retreat from Home, did not speci-
fically enjoin the pursuit of learning on his monks; but
they borrowed the idea at once from his contemporary,
the celebrated Cassiodoi-us, the real founder of monastic'
learning, of which his monastery of Viviers in Bruttiuia
is the first known school. But the most valuable feature
of the rule is the position of dignity which it assigns t#
work. It is scarcely possible to realize at the present daj^
the dishonour into which toil of all kinds had sunk in the
days of Benedict. Kot only had the institution of slavery
degraded many kinds of occupation, but the gradual
disajipearance from Italy of the yeoman class, ruined and
exiled by the concentration of great estates (latifundia),
or slain in the ceaseless battles of competitors for empire
or 6f barbarian invaders, left few save serfs and bondsmen
fo tijl the soil, while the military habits of the invading
tribes led them to contemn any life except that of a
warrior. It is the special glory of Benedict that hf
taught the men of his day that work, sanctified by prayer,
is the best thing which man can do, and the lesson^hae
never been wholly lost sight of since. . . ' «
The new institute spread with even more astonishing Spread
rapidity than the earlier monachism which it practically J"^__'°^'^,
supplanted in the West, and its history thenceforward is, ,i,jBens.
with one important exception, that of, Western conventual jictiue
life for some centuries. Moreover, besides marking the order?
close of the first or tentative ^ra of monachism, when all
kinds of crude essays and experiments were being made;
706
M O N A C H 1 S M
and being itself the beginning of a new and settled order,
it has the distinction of giving greater dignity and weight
to the female side of monachism than had been the rule
previously. Numerous and crowded as convents for
women were in the early church, there is little evidence
of their exercising any powerful influence as a factor in
the practical religious life "of the time, and though a few
individual women of eminence, a Euphrosyne or a Macrina,
illoitrate the annals of the common life in the East, yet
as a clafs the BasUian nuns do not yAay at all so important
a part in eccleFi.iRticai history as the spiritual descendants
■:!:' ScholaBtica, sic-ter of Benedict; for the same flexibility
and comparative gentlcncsa of his rule whicli made it
healthier for men than its precursors were &till more
erfective when dealing with the more sensitive organization
of women. Accordingly, the Benedictine nuns offer a
far greater variety of type than their Eastern sisters, and
exerted a much more visible influence upon society, even
before those newer forms of the organization of women's
work in the church were devised which have given it
much additional importance. Further, whereas the most
serious and well-founded objection alleged against mona-
chism is that by parting large companies of men and
women irrevocably from each other, and treating this
severance as an indispensable condition of the highest kind
of life, it has tended to throw discredit on marriage and
the family, and so to weaken society, which is based on
family life alone, a strong counter-plea can be put in for
the Benedictines. Not merely are they free, as already
remarked, from the anti-social tendencies of Oriental
monachism, which actually did disintegrate society in
Egj-pt, but their institute was the one corrective in the
early Middle Ages of those habits and ideas which tended
to degrade the position of women. The cloi-ster was not
alone the single secure shelter for women who had no
strong arm to rely on ; but it provided the only alternative
profession to marriage, and that one recognized by pubUc
opinion as of even higher distinction, and opening to
women positions of substantial rank and authority, less
precarious than the possession of temporal estates, which
might only serve to attract cupidity, and so invite attack.
The abbess of a great Benedictine house was more than
the equal of the wife of any save a very great noble ; and,
as single women were thus not obliged to look to wedlock
as the only path to safety and consequence, they were
enabled to mate on more equal terms, and were less likely
to be viewed as the mere toys or servants of the stronger
sex.
But the special eminence of the Benedictines, in which
they were without even tlie semblance of rivalry till the
Jesuits arose, is that they were a missionary, civilizing, and
educational body. It is true that the first successful efibrts
to convert the barbarian conquerors of the empire somewhat
jirecede their entrance on that field of labour, and Ulfila
amongst the Moeso-Goths, Valentinus in Bavaria, and Sever-
inus in Austria had achieved much even before Benedict
was born ; but their work needed to be taken u]) on a larger
.'-oale, and by a permanent organization not liable to bo
imperilled by the death of any one missionary or group of
missionaries. And the task of laying the very foundations
of civilized society, apart from the question of religious
conversion, was as yet quite unessayed. It was as teachers
of what for those times was scientific agriculture, as
drainers of fens and morasses, as clearors of forests, as
makers of roads, as tillers of the reclaimed soil, as archi-
tects of durable and even stately buildings, as exhibiting
a visible type of orderly government, as establishing the
superiority of peace over war as the normal condition of
life, as students in the library which thcirule set up in
tvery_ monastery, as the masters in schools open not
merely to their own postulants but to the children 6\
secular families al.so, that they won their high place in
history as benefactors of mankind. Uo d()Ubt there was
another side to this picture, even, befcre the order began
to deteriorate collectively ; but the good ;iotual)y eficcted
far exceeded the evils which may have accor/.panied
it. The Benedictine institute was carried to Sicily by
Placidus in 53-1 ; to France by Maurus, Simplicius,
and their companions in 543 ; to Spain at a somewhat
later and uncertain date ; but did not touch any of the
Teutonic countries till the very end of the century. That Tie Cel-
work was chiefly accomplished by another agency, that of t'l^^^e-
the Celtic monks, themselves disciples of a Christianity "*"*•
presumably carried to Ireland from Gaul, and following
a rule seemingly adapted from that of Pachomius. The
early history and constitution of Irish and Scottish
monachism are too obscure to be set down with any con-
fidence, but it is at least clear that it was mainly tribal
in oiganization, and even less subject to episcopal a;athority
than the Eastern and Italian forms. The same holds good
of the V\'elsh communities which survived the Saxon
invasions of Britain. Legend is abundant, trustworthy-
record is scanty, and only a few facts can be rescued from
obli\'ion. Amongst them may be included the introduc-
tion into Scotland of a species of monachism resembling,
that of Augustine, by Ninian, first missionary of the
southern Picts, who borrowed his institute from Martin
of Tours, and set up a cathedral, a house of canons, and
a school of learning at Vt'hithorn (Candida Casa) in
G".Iloway before the close of the ■1th century, himself
dying, it is thought, about 432 (.^Ired, Vit. Kin.). The
foundation of the second model of Welsh monachism
(the first has gone below the horizon of history) Ls
ascribed to the bishops Germanus of Auxerre and Lupus
of Troyes, who visited Britain in 429 to combat the
prevalent Pelagianism, itself a form of opinion due to a
British monk. They are alleged to have been, directly or
through their disciples, founders of great monasteries and
schools at Hentland on the Wye, at Llantwit, Llancarvan,
Docwiuni, Bangor, Whitland, &c. ; wliile among the more
famous names connected with these and similar houses
may be mentioned Asaph, David, Illtut, Dubric, Cadoc,
Gildas the Wise, and Kentigern, the last-named being a
zealous missionary. But Ireland was the true stronghold
of Celtic monachism, and before the close of the 5th
century was already thickly planted with religious houses.
Armagh, Clonard, Aran, Lismore, Cluain-ednech, Clonfert,
and, above all, Benchor or Bangor, the famous abbey of
Comgall, on the coast of Down, near the entrance of
Belfast Lough, are some of the more conspicuous founda-
tions ; and there are numberless stories recorded of the
learning, the austerities, and the miracles of their inmates.
The chief interest they have for the student of ecclesiastical
history lies rather, however, in the colonies they sent forth
than in their home operations, and it is to the great
foundation of Columba (521-597) at lona, the hive of
missions and home of Western learning, more than
to any Irish monastery, except Bangor, that the Celtic
raiil on heathenism is mainly due. The rule of Columba '
resembles the Benedictine in prescribing three kinds of
employment — praj'er, work, and reading ; while under the
last-named head not only Scripture but all attainable
secular learning was included, and it is also certain that the
work of cojiying JISS. in a careful and beautiful fashion,
which became so important a part of monastic occupation,
reached maturity first at lona. It remains only to say in
this connexion that the discipline of lena, apparently
borrowed from Irish use, made the abbot sujucme, not
~' PubU.shea l)y Dean Ufcves iu Colton's Viaitation oFvJ^ry, p. 109,
and in ¬)ier form by UaJiUu and Stubbs, Councils, tec, ii. p. 119.
M O i\ A C H I S M
r07
merely over Us monks, as in other rules, but over bishops
also, ■whose office v.as Eimply that of ordaining such as
were to be promoted to holy orders ; ' they had no
territorial jurisdiction as rulers, because the monastery,
not the diocese, was the primary local ujiit in Celtic Chris-
tianity, and thus a great founder or abbot was of more
account and power than a bishop. Another famous pupil
of Irish monachism, Columbanus, trained at Benchor along
with his companion Gallus, exercised a powerful influence
on the religious life of his time (543-615), not only
as the founder of important monasteries at Luxeuil,
Fontenay, and Bobbio, and as scholar and missionarj', but
also as the author of a rule, more severe both in its pro-
visions and in its penalties than the Benedictine, with
which it disputed for a considerable time the first place,
and which it might very probably have displaced, had not
the Benedictine institute, as of Italian origin, found that
favour at Rome which a Celtic code, bearing more than
one trace of divergence from Latin usages, could scarcely
expect. With the mention of another prominent name in
ihe list of distinguished Celtic reformers and mission-
aries, that of Fursey, abbot of Lagny neai- Paris (c. 650),
we close this sketch of the Celtic movement in the 6 th
and 7th centuries, merely adding that it^ extent and
influence may be partly estimated from the number of
monasteries founded in England and various parts of the
Continent by Irish monks, and the list of Celtic saints
recoverable from the dififerent martyrologies and similar
records. The former amount to more than one hundred ;
the latter to nearly three hundred.
Kcturning to the Benedictines, the most important event
in their history after the consolidation of their institute
was the favour they received from Gregory the Great,
himself once a monk, who set himself to reform monastic
discipline, then at a very low ebb save where the new
foundation was at work. He enacted several regulations
for the better government of monasteries, such as pro-
hibiting the admission of any persons under eighteen,
exacting two years' novitiate, enforcing inclosure, visiting
relinquishment of monachism with imprisonment for life,
and finally, in the Lateran synod of 601, exempting
monasteries in all cases from the jurisdiction of bishops (a
measure due, it appears, to episcopal misconduct and
oppression rather than to monastic ambition), thereby
abolishing the measme of control which the eighth canon
of Chalccdon and the legislation of Justinian I. in 535
had loft in the hands of the diocesan, and leaving only
the still surviving check, that the bishop's consent was
required for the erection of any new monastery. The
mission of tke monk Augustine to England in 596 was,
however, destined to produce more immediate and for-
tunate results than this piece of legislation. It brought
Latin monachism into a part of Britain whence Welsh
monachism had been long extirpated, and though little
success attended the original foundation at Canterbury,
yet two other houses were destined to be the cradles of
great things. Jarrow-on-Tyne, founded by Benedict Biscop,
trained the illustrious Bede, to w^hom is due the monastic
school of York, which in its turn sent out Alcuin to recon-
stitute European learning under the fostering hand of
Charlemagne ; Nutcell in Hampshire reared Boniface to be
the apostle of Germany, and founder of one of the most
celebrated and powerful monasteries of the Middle Ages,
that of Fulda. Nevertheless, decline set in very soon.
> So Bade tells us: "Habere autem solet ipsa insula rectorem
seiaper abbalem presbyterura, cujus juri et omnis proviucifl et ipsi
tti.'vjn episcopi, online inusitato, debeiint esse subject], juzta exemplura
prinii doctoris illius, qui non episcopus sed presbyter extitit et mona-
chus" {Hist. F.cd., iii. 4); tliougb, after all, the principle is precisely
that of tlie Beuedictiue rule as applied to priests.
and the Sth centxiry was a time of deterioration amongst
both the seculars and the regulars. To amend the forn^er, Monastia
Chrodegang, bishop of Metz, instituted in 760 an order r«fonn-
of Canons Regular, living by a rule carefully based on and "^^
adapted from the Benedictine, >vith the bishop as abbot, ° ^'^'
the archdeacon as prior, and with a general likeness in all
the details of community life, except that there was no
obligation to poverty, and the canons were allowed to
enjoy any private property and such fees as they might
receive for the performance of religious rites. Tliis rule
became extremely popular, was sanctioned by the coun-
cil of Aix-la-Chapelle in 816, and was adopted in most
cathedrals of France, Germany, and Italy v.-ithin fifty
years after, besides making some way in England aiso.
It prevailed till the institute of the Austin Canons was
substituted for it. And, as regards the laxity amongst
regulars at this time, there is extant a very interesting
letter from Bede addressed to Eegberht, archbishop of
York, calling his attention to the excessive number of
monasteries in northern England which were conducted
without a rule, and were often merely fictitiotis institutions,
founded by laymen with the object of obtaining charters
of privilege which would exempt them from civil and
military burdens, — such laymen then assuming, without
warrant, the title and powers of abbots, and filling their
houses either with monks expelled from their own societies,
or with lay retainers induced to receive the tonsure and
promise obedience. Bede calls on the archbishop to con-
vene a sjTiod and institute a visitation for the correction
of these abuses. The cause of the decline of the monasteries
is to be sought in their popularity, which brought them
great estates and other kinds of wealth, leading to the
relaxation of the vow of poverty, which was interpreted
as merely forbidding individual property ; in the growth
of pluralities ; and in yet another cause which at first does
not seem to lead in the same direction- — the growing
custom of ordaining monks, hitherto laymen, to fit them
better for missionary work. But this led, not only to
much more intercourse with the society of a lax and
turbulent age than suited with claustral niles, but to
ambition, as it became customary to fill several sees with
monks from certain abbeys. The declension, notably in
the habits of the superiors of wealthy houses, had become
very marked, when a reformer arose in the person of a
second Benedict, of Aniane in the modern department of
the Herault (750-821), who, in gratitude for an escape
from drowning in the Ticino in 774, adopted the mon-
astic life, and changed his name Witiza to that of the
great Nursian monk. But he accoimted the Benedictine
rule too easy, and adopted instead the severest practices;
of Eastern monachism. He quitted the house of Seine,
where he had be'en professed, and betook himself with a
couple of companions to Aniane, where by 782 he had
built a monastery for a thousand monks, with depend-
ent cells, and collected a considerable library, paying
special attention to the acquisition of the rules of the
different monastic bodies both of East and West. He was
transferred by his warm patron, the emperor Louis the
Kdus, to an abbey built for him near Aix-fa-Chapelle,
whence he acted as in some sense a superior-general and
inspector of all the Benedictine houses, and drew up a
harmony of all the rules he had collected to aid him in
the task of reform. What he actually effected was the
practical abolition of most of the competing codes, so as
to leave the Benedictine in nearly sole possession, and to
procure the enactment of a large body of tanons in the
council of Aix-la-Chapelle before mentioned, which laid
down detailed provisions for the government of monasteries,
whose very minuteness made them vexatious and •ulti-
mately intolerable, so that the reform lasted scarcely tw«i
70S
M O N A C H 1 S M
generations trom its inception. 'Parallel mth the time of de-
clension and partial reform just described was the rise and
decay of the noble and far-sighted school-system projected
by Charlemagne, and entrusted to the superintendence
of Alcuin. Its relation to monachism as distinguished
from the history of education, is that one of its main
features was the capitulary of 789, which directed that,
besides the primary school attached to each monastery,
all the more important houses were to found and open
secondary ones also, with a higher range of subjects, even
if such schools were interior or claustral, and only for
the junior monks and novices, not exterior and free to the
general public. Several of these schools rose to consider-
able efficiency and repute, notably those of Fulda, St Gall,
Tours, and Eheims, discharging to some extent the
functions of universities. But the weakness of the later
Carolings involved this plan in the troubles which ended
in the break-up of the empire of the Franks, and the 10th
century saw the end of it. In England monachism shared
the common destiny of decay. It had been marked during
the period known as the Heptarchy by a degree of royal
favour unparalleled elsewhere ; for it may almost be said
that the number of kings, queens, and persons of royal
race who here betook themselves voluntarily to the cloister
— and not under political compulsion, as often in con-
temporary France — exceeds the aggregate of those in all
other countries. Yet it is likely that the fashion set in
this wise helped to hasten decay, by inducing many persons
to adopt the monastic Ufe vdth little taste for its restric-
tions ; and it is certain that secularity (chiefly manifesting
itself in costly dress), riotousness, and drinking had become
frequent amongst the English monks of the 8th and the
early part of the 9th century. The decay was further
precipitated by the spread of the institute of Chrodegang,
which thinned the supply of recruits to monachism proper,
as the easier life of canons regular w.as preferred. The
same cause affected the convents of nuns, for an order of
canonesses was established about this time on similar line^.
The one bright spot in the history of 9th century mona-
chism is the conversion of Sweden by Anskar, a monk
trained in the famous house of Old Corbie in Picardy,
which, albeit Benedictine, had been mainly planted by a
colony from the stricter Columbanian house of Luxeuil,
and had thus kept the traditions of a purer time almost
unimpaired.
The 10th century ^-emphaticaNy the "Dark Age" or
" Age of Lead " — was the tims when monachism, both in
East and West, touched its lowest point. Three causes
contributed to this in the West : — first may be placed the
raids of the Northmen ; next, the gro^vth of the feuda'
system, converting abbots into secular lords in virtue of
the lands held by their monasteries being chargeable with
feudal obligations; and lastly, the seizure and impropria-
tion of monastic revenues by kings, princes, and bishops.
The last of these causes was at work in the East also,
further complicated, as we learn from the decrees of a
council held at Constantinople in 861, by the founda-
tion of monasteries intended from the first merely as
sources of pecuniary advantage to the founders; although
the success of Greek monks in the conversion of Bul-
garia, Moravia, and, somewhat later, southern Russia,
showed that the cloister had not become quite effete
even under the conditions of the Byzantine emcire in
that era.
Wliat the state of things was in the West, even at the
outset of the 10th century, may be learned from the
language of the council of Trosley, near Soissons, in
909. It speaks of the ruin of many abbeys by the
heathen, and of the disorderly condition of many which
survived. Monks abandon their profession ; married lay
aoDots, witii guaras ^nd hunting retinue, occupy - tJifi
cloisters of monks, canons, and nuns ; and the rules are
universally disregarded. But, as constantly before,' sp
then, reformers were at hand. Berno first abbot of Cluny
in France, Dunstan in England, and, somewhat laterj
Anno archbishop of Cologne in Germany, undertookj
and to a considerable extent effected, the work of reform/
Only the first of these, however, calls for special notice
here ; and it will suffice to say that Berno, after having
been abbot of Beaume, was set by William the Pioufij
duke of Aquitaine, over his new foundation of Cluny in
910, where he speedily initiated a reform of the Bene'
dictine rule, whose very name, and even the memorj
of the reforms of Benedict of Aniane, had been forgotten
in nearly all the so-called religious houses of the time.
This new rule is the first example of the establishment of
an order within an already existing order, of which it still
formed part, many subsequent instances of which occur
later. It was stricter than the original code in several
particulArs, notably as regards fasting and silence ; and it
laid especial stress on liturgical splendour. Cluny became
the head of a large number of dependent houses, and,
under the government of Berno's successors, Odo, Aj-mard,
Majolus (who refused the papacy), Odilo, and Hugh I.,
rose to great eminence, but was nearly brought to ruii
by Pontius, abbot in 1109, who was soon deposed, and
succeeded by Hugh II., and then by Peter the Venerable,
who completed the work of di-afting the statutes of thp
new order, begun long before, but not finished, by his pre
decessors. In his time (1093-1156) the Cluniacs spread
over not only the whole of France, but had houses ir
Italy, Spain, England, Palestine, and in Constantinople
itself, and the "Arch-Abbot," as he was called, had more
than 300 churches, colleges, and monasteries under his,
authority. It is enough to say, with regard to Dunstan^
reforms in England, that they were directed to two objects'
the substitution of monks for secular canons, and th(
introduction of the Benedictine rule, till then practicallj
unknown in England, into the monasteries, — for the mona'
chism introduced by Augustine belonged to an earlier
type.
The 1 1 th century is noticeable for several events in the Ne\r
liistory of monachism ; first of which stands the foundation orders,,
of the Order of Camaldoli by Eomuald, early in the 11th J^J^'^-'^'*
century, a strict community of hermits, living by the
system of an Eastern laura of detached cells; but this
society has never been of much importance. The Ordei
of 'Vallombrosa, founded by John Gualbert in 1039, is
more remarkable, as being the first to introduce the
grade of " lay-brothers," which plays so large a part ir
later monastic annals, — the object being at once to open
the cloister to a class previously barred by the obligation
to recite the oflice in choir, which necessitated a certain
degree of education, and to lighten the strain on the
choir-brethren by relegating the rough work of the monas'
tery to an inferior grade of inmates, thus securing more
time for reading and meditation for the cultured monks)
A series of struggles between bishops and abbots in this
century in respect of monastic jurisdiction-^the practice
having constantly vacillated in desjiite of Gregory ihl
Great's decision 400 years earlier — issued mainly, thougl
not wholly, in favour of exemption, and the reforms pusheo
everywhere rehabilitated monachism in pojiularity. The
great stimulus given to the spirit of ecclesiastical dia
cipline and energy by the Hildebrandine movement con
tinned not only during the reign of Gregory VII., but fo;
a considerable time after : amongst its results were the
Order of Grammont, founded in 1074, but not transferred
to the place whence it is named till 1124; the far mors
celebrated and influential Carthusians, a peculiarly ascetic
I
!V1 O N A C H I S M
"09
cctnmunity, established by BVuno at ?ne Chartreuse, near
Grenoble, in 1084, which still boasts that it is the only
order which has never been reformed on the ground of
deviation from its original institute ; and the Order of
Fontevraud, founded for both monks and nuns (more
strictly, canons and canonesses) by Robert of Arbrissel in
1100. Kegarding the last named two remarkable facts
may be cited : that the founder in 1115 entrusted the
superior-generalship of the whole institute to the abbess
of the nuns ; and that he provided that new abbesses
iShoXild always be elected from secular women, as having
more practical knowledge of affairs and capacity for ad-
ministration than women trained in a cloister. There is
yet one order more belonging to this period of new
! foundations, of higher note than most — that of the Cister-
cians, founded by Robert of Molesme in 1098 at Citeaux,
near Dijon. This society, chiefly famous as that to which
Bernard of Clairvau-i: belonged, carried its asceticism into
a region whence the other monastic bodies had banished
it, that of Divine service. The barest simplicity in build-
ings, chtirch furniture, and worship was unjoined by the
rule : plain linen or fustian vestments, iron chandeliers,
brass or iron censers, no plate save a chalice and a tube
(and those of silver rather than of gold), no pictures, stained
glass, or images, and only a few crosses of painted wood,
and the most rigid simplicity in chanting, — such was the
ceremonial code with which they challenged the costly ritual
of Cluny. A more durable innovation was the institution
of " General Chapters," to which every abbot of a Cistercian
house had a right to be sximmoned to sh.are in the delibera-
tions held at the chief establishment, and which he was
even bound to attend, that, while each dependent house
thus obtained a representation in the parliament of the
order, it could be called on to render to the central authority
an account of its om~;i doings. The Austin Canons, already
mentioned, were probably founded at Avignon about 1061,
and the Order of PnSmontriS by Norbert in 1120. This
society was simply a stricter body of Austin Canons, stand-
ing towards them much as Cluny did to the Benedictines.
But there are yet two other institutes of this active period
which differ from all previous foundations. So far, the new
orders are merely modifications, more or less sweeping, of
the original Egyptian system, but the crusades gave birth to
two entirely unprecedented forms of monachism : — the Mili-
tary Orders, of which the most celebrated are the Templars,
the Hospitallers, and the Teutonic Knights ; and convents
of women, affiliated to these orders, who were appointed to
serve ui the lazar-houses, hospitab, and similar institutions
attached to them, and whose rule, for the first time in
monastic history, was drawn up on a distinctly active and
not a contemplative basis. Work of the sort had been done
long before, but only as a casual accident, not as the primary
object of a community.
Militjry The military orders arose in a more accidental fashion
wilen. than any other variety of monacliism, being duo to the
desire felt to lessen the perils which attended pilgrimage
to Jerusalem, then almost as much part of the religious
craving of Christendom as the hajj to ilecca is with devout
Moslems. 'The Templars v.ere at first designed only as an
armed escort to protect the visitors from attack, ar.d the
idea of permanent guardianship of the Holy Places did not
shape itself till later; while the Hospitallers (afterwards
famous as Knights of Rhodes and of Malta, as the main
bulwark of Christendom against the Turks, and as main-
, taining the police of the Mediterranean against all pirates
and rovers), borrowed the first idea of their institute from
the knightly order of St Anthony of Vienne, founded in
Dauphin^ aboutd095, and devoted themselves originally to
tending sick pilgrims at Jerusalem. The Teutonic Knights
date from the third crusade, and owe their foundation to
the sufferings of the duke of Swabia's anuy at the siege
of Acre, as it would seem that the Hospitallers were either
unable or unwilling to supply the needed assistance. These
knights, when at last the Eastern crusades were abandoned,
turned their arms against the heathen of Prnssia, which
they conquered, as also Livonia, Comiand, and Pomerania,
besides keeping the Slavonic enemies of Germany in check
by frequent raids into Lithuania and Poland, holding their
gi'ound as a sovereign order for three centuries, till tho
Reformation brought about their fall. The common char-
acteristic of all these orders was tho union of the seemingly
incompatible qualities of the monk and the soldier in tho
same persons, of the' convent and the barrack in the same
house. But the contrast was not so sharp to mediaeval
eyes as it would be to modem ones ; for while knighthood
was surrounded with religious ceremonies and sanctions on
the one hand, and on the other the feudal rank of bishops
and abbots made them in some sense military chiefs, occa-
sionally even taking the field in person, there was no great
difficulty in accepting the permanent combination of what
was often found casually united. The military orders passed
away when their work was ended : the Templars, as the
victims of a great crime, closed by a ghastly tragedy ; tho
Hospitallers, and those Spanish and Portuguese orders which
were enrolled as regiments against the Arab invaders of the
PeninsvJa, though titularly stOl existing, yet really ceased
to be more than a name when the Moslem power in Europe
was finally broken. But the active organization of women
was a more fruitful germ, and has never since ceased to
put forth new developments, varying with the notjced want.-i
of each period. To this epoch belongs also the beginning
of that policy of the Roman see of utilising the monastic
orders, won over by special privileges and exemptions, as a,
body of supporters — almost a militia — more to be relied on.
than the secular clergy, and thereby the seed of conflict
between seculars and regulars, destined to work much evil
later, was sown, and also the beginning made of that dena-
tionalisation of monachism which tended from the fixst to
its unpopularity and decay.
It was found that a new order was the best safety-valve
for enthusiasm which might become dangerous if dis-
couraged, but which could be made a valuable ally if
allowed to take shape in a fresh society, hoping to surpass-
all its precursors ; and it is worth remarking that the one
occasion when this wise policy was departed from, when
Peter Waldo vainly sought in 1 179 recognition and sanction
from Pope Alexander UI. for his proposed institute of
mission preachers, gave rise to a sect (the Waldenses)-
which is stiU existing, and which has given trouble to the
Roman Church quite disproportionate to its numbers and
influence. The Carmelites, founded by Berthold of Calabria
on Mount Carmel about 1180, and incorporated under rule
by Albert, Latin patriarch of Jerusalem in 1209, were the
last order of importance which sprang up at this time ; for
the Gilbertines, an English order founded at Sempringham
in Lincolnshire in 1H8, curious chiefly for their double
monasteries for men and women; the Beguines, c. 1170
(who are, however, notable for their semi-secular and
parochial organization, whence many later active bodies
have borrowed hints); the Humiliati, c. 1196; and the
Trinitarians, for the ransom of captives amongst the Moors
and Saracens, founded by John de JIatha and Felix do
Yalois in 1197, never rose M great influence or popularity,
though the Servites, an order of the year 1223, became
powerful in Italy. This period of rapid multiplication
was quickly followed by one of equally rapid decay,
the first to show clear tokens of degeneracy being the onco
rigid Cistercians, who never recovered their old moral foot-
ing, and who, it may be mentioned, were accountable for
much of that hatred of tb" f^lhurch of the Pale in Ireland
710
M O :^ A U H i S M
by the natives, which, given ffOih fuel by the Seformation,
has lasted to the present day.i
Menai- Yet another fresh departure in ths history of monachism,
cant in some respects the most momentous of all, was taken in
Orders, ^-^^ j gth century hy the institution of the Mendicant Orders,
flitriars- ^^ j,^..^^^^ p^^^ Innocent m., in the 13th of the 70
constitutions Oi- canoes he promulgated at the Latei'an
council in 1215, had expressly forbidden the foundation
of any new orders, bidding all ■who desired to embrace
th" monastic life join some approved community, and
similarly directing that such as desired to found new
houses should take their nile and constitution from one of
the recognized societies. But circumstances were too strong
for iim, and this very pope was destined himself to sanction
two of the most remarkable societies which the Latin
C!hurch has ever produced. The time was an anxious one.
The speculative activity of the age, coupled -n-ith the abuses
in the chiu'cli, was multiplying sects, formidable in numbers,
and still more from the contrast their austere mode of life
prei;ented, not only to that of the secular society of the day,
but to that of the ecclesiastics, notably those of rank,
whose pomp and luxury gave rise to the first faint stirrings
of a revolutionary spirit amongst the commons, which the
gre'.it pope, who was then the most conspicuous figure in
Europe, did not fail to observe. No effectual weapon of
leoistance seemed at hand ; the parochial clergy, yielding
to the difficulties which an iiclated rural life throws in the
W3,y of intellectual effort (far graver then than even now),
had almost everywhere sunk into sloth and incapacity ; the
monastic orders were content, in the better instances, with
maintaining theii- own internal discipline, and had no surplus
energy for external work, while in the worse examples (as
in that of tlie Cistercians, just referred to) they served
rather as beacon?, of v/arning than as patterns for imitation ;
and, in short, there was an ever-increasing mass of home
mission work to be done, and no one to do it.
rsut the two men who were to do it were already at
hand in the persons of Francis Bernardone of Assisi and
Dominic Guzrnau of Osma. The ruling idea in the mind
of the former was the elevation of poverty to the first
place amongst Christian graces, as the most obvious way
of conforming the life of a Christian to that of the founder
of his faith ; the more intellectual Spaniard dreamed of
an aggressive body of skilfully-trained preachers, able at
once to grapple with the subtle dialectic of the enemies of
the established creed, and to appeal in clear and homely
language to the uneducated, amongst whom the AJbigensts
and other sectaries were making considerable conquests.
Francis,, the poet and devotee, in renouncing even the
scantiest provision which the strictest orders of his time
securf,d for their members, and bidding his followers to
live on alms daily begged, taking, in the most literal sense.
1 There is a .ery curious letter from Arunlf, bishop of Lisieux, tv
Pope Alexandur III. (1159-1181), asking him to dissolve the Benedictine
abbey of Grestniu in that diocese, and to dr.ift its inmates into other
houses, which illustrates both the kind of abuses which were sometimes
found and the desire of the autlicritics to suppress them. He charg-js
the monks with lack of charity and hospitality, in that they reserved
even the broken scraps from the common table as perquisites for their
private friends ; that they habitually quarrelled, and wounded one
another with their knivta, being prevented from homicide only by the
knife-blades having no point ; that one monk had actually murdered
the cook, who had complained of his visits to the cook's wife ; that the
abbot did not provide for the daily wants of the community, but allowed
the monks to roam abroad, picking up food for themselves as best they
might ; that some of them had caused the death of a sick woman by
plunging her into ice-cold water under pretext of working a miraculous
cure J that the abbot was frequently absent on pretence of business,
hut really living a loose life ; that ho had been thus two years in
England, till recalled by the bishop, who was forced to send him awny
dgain, after appointing a deputy ; that this deputy, when drunk, had
•wounded two of the monks, who thereupon mnr lored him ; so that the
(loase was practically pr.st reformation, and ought to bo dissolved.
no thought for the morrcTC, appealed to the iwpnli
imagination, always ready to Hndlo at the sight of genuica
self-sacrifice ; Dominic, with not less insight as a thinker
whose first care vras for doctrin:il orthodoxy, as that of
Francis was for personal piety, saw that there was a
demand ready to sjirii-.g up for more exact and intelligent
religious teaching th?n could then be had, cave in a few
great cities. The occa-siou which urged him to the task
he Vindertook is noteworthy. Hs had long been a canon
of Osma, the strictest and sternest member cf an ascetic
community, when in 1203 he had to go en a journey with
his bishop, which brought them into the very midst of the
Albigenses in. the county of Toulouse, where they saw how
powerless the clergy ware to contend against their rivals.
On their road home the bishop and Dominic met the
three papal legates returning discomfited from Languedoc,
but attended with as much pomp as a triumphal progress
would have justified. Dominic rebuked them sternly, tell-
ing them that it was not by splendid retinues and costly
garb that the heretics won their converts, but by zealous
preaching, by humility, by austerity, and by at least
seeming holinecs. Both the now founders sought and
obtained at Kome, after some difficulty, the approval of
their new institutes, and that in the very yeor 1215 which
had seep the formal prohibition of all fresh orders.
Francis speedily returned to his home, but Dominic, whose
idea had by this time expanded from that of converting
merely the Albigenses of Provence and Languedoc to that
of influencing the whole world of nominal Christians and
outer heathen, settled himself in Rome, where the pope
appointed him to the important office of Master of the
Sacred Palace, which has ever since been held by a
Dominican, and carries with it the authority of chief
censorship of the press. The two new foundations
borrowed from each other, Francis copying Dominic's
scheme of itinerant preachers, and Dominic imposing on
his disciples the mendicant poverty of Assisi. These two
particulars, the total absence — at any rate at first — of such
endowments as had proved a snare to the older societies,
and the substitution of itinerancy for inclosure, are the
features which distinguish the friars from the monks who
preceded them. The Franciscan institute was a bold
attempt to democratize the church ; Dominic's Friar
Preachers, though recruited freelj' from men of a humble
grade, have always had somewhat more of an aristocratic
tone about them, due to tlicir intellectual calling; they
have held a high place in Christian art, counting amongst
them such names as Fra Angelico and Baccio della Porta ;
and their reputation for orthodoxy and for a purer type
of moral theology than the Jesuit one has always stood
high. They also count amongst their members the two
most eminent divines of the Middle Ages, Albertus
Magnus and Thomas Aquinas, and they have been fruitful
in producing zealous missionaries ; but the or e L,reat blot
on their career is that they have been the directors and
ofSciols of the Inquisition ever since the formal constitu-
tion of that tribunal as a permanent organization. The
Franciscans, less distinguished for mental triimiphs than
their competitors, have yet some famous names ch'ef of
which are Duns Scotus and Roger Bacon. — lor Pc/iaven-
tura, though set by the Franciscans as the " Sirr.phic
Doctor" in competition with Aquinas, the "Angelic
Doctor" of the Dominicans, is scarcely entitled to very
high intellectual rank — and at one time they seemed likely
to establish as firm a hold on the university of Oxford as
the Dominicans did on that of Paris. The swiftest success
and popularity attended the two new orders ; privileges
■and exemptions were showered on them from Rome ;
wealth, in despite of their vow of mendicancy, was
emulously thrust upon them by the laity ; and, above alljj
M O In A C H 1 S M
711
a remarkable and widcsjiread religioas reviva', a dead-lift
to ministerial efnciency in every direction, repaid their
early labours, while they had between them almost a
monopoly of the popedom for nearly two hundred years.
And one peculiarity of their organization gave them a
degree cf strength which no other orders possessed. ■ Each
monasti.ry of the older societies was practically isolated
and independent of all others, unless it were itself a
dependent priory or cell belonging to a greater house.
Some societies had, it is tiue, general chapters, but these
were rare, and at best only effectual in establishing a
certain uniformity of practice in all houses of the same
-.no. But the Friars, like the Templars and Hospitallers of
Sin earlier day, and like the Jesuits of a later one, were
enrolled in something of military fashion, under a superior-
general, ^vith wide powers, who directed and controlled
'heir actions from one central point. Every group of
neighbouring friaries was formed into a congregation,
under a local head or provincial, and he was always in
direct communication with the general, so that a common
government united the whole body into a compact mass.
But their very success was fatal to their character. The
vow of poverty was the first part of their institute to
break donm. Even before they began to be counted
amongst the richest orders of Christendom, there is
indisputable evidence — that of Bonarentura, himself
general of the Franciscans — that the mendicant system
was working nothing but mischief. He tells us, writing
while the order wis still very young, and within fifty
years of the founder's death, that it was even more en-
tingled in money cares and business concerns than the
endowed communities, precisely because there were no
funds available to fall back on in emergencies ; that the
brethren, discouraged from work by mendicancy, were
habitually idle ; tliat they roamed about in disorderly
fashion under pretext of questing ; that they were such
brazen and shameless beggars as to make a Franciscan as
much dreaded by travellers as a highwayman ; that they
made undesirable acquaintances, thus giving rise to evil
reports and scandal ; that conventual offices had to be en-
trusted to imtried, unspiritual, and incompetent brethren ;
that vast sums were lavished on costly buUdings ; and that
the friars were greedy in the pursuit of burial fees and of
legacies, so that they encroached upon the rights of the
parochial clergy. If such were the mischiefs at work before
the first zeal had begun to cool, it may readily be gathered
how entire Avas the failure at a later time. Indeed, as
regards the Franciscans, not only did they endeavour to
evade the stringency of their institute even in their
founder's lifetime, but the whole society was soon divided
into two hostile camps, one of which desired to adhei-e
closely to the original rule, v/hile the other was content to
fall in with the habits of the " possession ers," as they had
been wont contemptuously to name the endowed orders.
And what is very curious in this connexion is that the
friars who were loyal to the principle of poverty broke
away for the most part from the church, forming new
sects, such as the Fratricelli, or attaching themselves to
elder ones, like the Beghards and the Apostolici, which
handed on in secret the Gnostic traditions of the third
century, apparently stamped out in the crusade against
the Albigenses, while those who openly disregarded the
will of their founder remained steadfastly in the Latin
church. No order, except the Benedictines, has had so
many branches and reforms as the Franciscans ; amongst
which it will suffice to name the Capuchins, the Minims;
the Observants, and the Recollects ;. while the Poor
Clares, the nuns of the institute, have also divided into
■Clarissines and Urbanists. The institution of Tertiaries,
seculars affiliated to the order as honprary members, while
continuing to live in the world, and P.dopting a certain
modified daily rule, was a powerful factor in the success
and strength of the order, and was adopted, but with less
conspicuous results, by the Dominicans. The rivalry of
these two great bodies with each other, prolonged with
much bitterness for centuries, and their disputes with the
parochial clergy, whom they long displaced in general
repute and influence, belong rather to general church
history than to the annals of monachism, and may be
passed by with this brief allusion ; while it suffices to say
that all the support they, and the other less important
communities of the same kind, such as the Carmelite and
Austin Friars, received from the popes, whose most effective
allies they were in every tountry where their houses were
found, was not able to avert their decline in general
estimation ; and there is no f.gure in later mediaeval
literativre on which the vials of contempt and indignation
are so freely poured as on the begging friar, and that, it
must be said, deservedly.
As the 1 3th century is the apogee of later monachism. Decline
so the decline begins steadily at the very outset of the of moo*
lith (which is also the date of ordination becoming the '^'''*'"'
normal custom for choir-monks, instsad of the exception, . . ^'"''
as formerly), continiung down to the crash of the Keforma-
tion.i The great schism of the West, the rise of the
Wickliffites and Lollards in England, and of the body
later known as Hussites in Bohemia, could not fail to act
injuriously on the monastic orders ; and, though the
creation of fresh ones continued, none of those founded
during this era were influential, and few durable. It
will suffice to name some of the more prominent : — the
Olivetans in 1313, who were rigid Benedictines ; the nuns
of Bridget of Sweden in 1363, who followed a rule compiled
from those of Basil and Augustine ; the Hieronymite
monks in 1374 ; the Brethren of the Common Life,
founded by Gerard Groot in 1376, who did much for
education and in home mission work, but are chiefly
famous now in virtue of one member of their society,
Thomas a Kempis ; the Hieronymite Hennits in 1373-1377 ;
the Minims in 1435; the Bamabites, a preaching and edu-
cational order, in 1484; the Theatins (a body of Clerks
Regular who aimed at little more than raising the tone of
clerical life, made but slight pretension to austerity, and
are, indeed, mainly noticeable as having suggested to Igna-
tius Loyola several points which he adopted in regulating
the mode of life to be pursued by the members of his
institute) in 1524 ; and the Capuchins in 1525.
In the Reformation era itself the monastic bodies had
sunk so low in the estimation of even the rulers of the
church that one clause in the report of the committee of
cardinals appointed by Pope Paid III. (a body composed
of Sadolet, Contarini, Eeginald Pole, Giberti, Fregoso,
Badia, Aleandro, and Caraffa, afterwards Paul lY.),
delivered in 1538, was worded as follows : —
" Aaother abuse which needs correction is in the religious ordera,
because they have deteriorated to such au extent that they are a
grave scandal to seculars, and do the greatest harm by their
example. We are of opinion that they should bo all abolished,
not so as to injure [the vested interests of] any one, but by forbidding
them to receive novices ; for in this wise they can be quickly done
• Tbe lang-joge of Nicolas de Clamenges (1360-1440)— rcttor of the
university of Paris, known as tlie " Doctor Theologus " — in his treatise
Be Corrupio EccUsim Statu, paints tbe moral decay of tlio monastic
bodies, and especially of the Mendicants, in the very darkest colours.
He not only charges them with waste, idleness, gluttony, drunkenness,
and profligacy, but alleges the condition of convents of nuns to be sucb
that there was little practical difference between allowing a girl to take
the veil and openly consigning her to a life of public vice. And the
Jievdations of Bridget of Sweden (1302-1373), approved by the coun-
cils of Constance and Basel, and by Popes Urban VI., Martin V., and
Paul v., fiUly confirm the darkest features of this testimony as regudj
the religious houses of the 14th century.
712
M O 2^ A C H 1 S J\I
away with without wrong to .my inc, and L'ood religious can be put
in their place. At present we tliiiik the best thing to be done is
to dismiss all the uuprofessed jouths from their monasteries."
As this formal document showed the current of high
ecclesiastical opinion, so the lay view took expression in
the Epistola, Obscurormn Virorum of Ulrich von Hutten,
which was to the Dominicans of the 16th century almost
what the Proiincinles of Pa.scal were to the Jesuits of the
17th ; while they came also .nder the more delicate scalpel
of Erasmus's wit. Not that the objections were wholly
new, for it is evident from Thomas Aquinas's defence of
monachisru against its detractors that they were nearly all
dsed in the 13th century. The interests involved were,
however, too vast and complicated, the supposed impolicy
of an admission on so large a scale of the charges alleged
against monachism by the men of the New Learning too
serious, to allow of any such sweeping measure of reform
as that proposed by the cardinals being carried out. A
certain amount of discouragement shown towards the older
societies ; the enactment of some partial corrections by
the couDcU of Trent, not touching any principle whatever,
but apparently saying something because public feeling
looked for something to be said ; and, above all, the crea-
tion of a new type of order, the famous Company of
the Jesuits (1534), represent the total action taken by
the Roman Church during the actual crisis of the Kefor-
mation. Apart from such direct revolts from the Latin
obedience as those in Bern, Zurich, Denmark, and Sweden,
which at once involved the monasteries in the general
overthrow of the old system of things religious, the most
remarkable proceedings in the reaction against monachism
were those taken in England, at a time when no breach
with the Roman Curia was thought of. So far back as
the 13th century Kings John and Edward I., and yet
again in 1337 Edward HI., had confiscated the "alien
priories," as those houses were called which were depend-
encies of foreign monasteries, and the last named let out
their lands and tenements until the peace with France in
1361, when he restored their estates; and similar raids were
made on them both in his reign and in that of Richard II.
Henry LV. showed them more favour; but in 1410 the
House of Commons proposed the confiscation of all the
tempoialities held by bishops, abbots, and priors, petition-
ing the crown to employ their revenues in paying a
standing army of knights and soldiers, in augmenting the
incomes of some of the nobles and gentry, in endowing a
hundred hospitals, aud in making small yearly payments to
the secular clergy. This fact attests the imix)pularity
of the church and the religious orders at the time, and,
though the large scheme was dropped, yet in 1416 parlia-
ment dissolved all the alien priories, and vested their
estates in the crown. They were for the most part
applied to ecclesiastical purposes ; but some portion, at
any rate, pass»d into private hands, aud was permanently
alienated. Hence there was nothing to create sm'prise,
much less opposition, when Cardinal Wolsey in 1523
obtained bulls from the pope authorizing the suppression
of forty small monasteries and the application of their
revenues to educational foundations, on the plea that
these le.-i.ser houses were quite u.seless, and not homes of
either religion or learning, whereas a learned clergy was
imi>cratively needed to combat the new religious opinions
which were making rapid way. And that the monasteries
had been subject to serious vicissitudes all along apjicars
from the fact that only about one half of all the founda-
tions known to have been made in England were in
existence at the date of the dissolution. There is little
reason to trust the charges of immorality brought against
the monks when Henry XHl. had once resolved on the
Jiilloge of the monasteries, seeing Low the path opene-I
by Wolsey could be followed up. The characters of tho-
king himself, of Cromwell, his chief agent in the disso
lution, and of Layton, Legh, and others of the visitors
appointed to inquire into the condition of the houses, arc
such, as to deprive their statements of all credit ; and,
besides, the earlier Act of dissolution, granting the smaller
monasteries to the king, limits the chaiges of misconduct
to them, expressly acquitting the laiger houses. Never-
thelesf?, when the apjietite for ]>hmder had increased with
the first taste of booty, accusations of precisely the same
sort were brought up against the gr<:at monasteries,
though in no instance has any verifiable )iioof been pre-
served.' But there can be no reasonable doubt (especially
"in view of the visitations of Archbishop Warhara and other
pre-Reformation prelates), that the religious houses, viewed
simply as corporate estates, had been very badly managed
for a considerable time, were heavily encumbered, and a
v,-eight round the neck of financial piogress in England;
and that, as spiritual agencies, they had mainly outlived
their usefulness, so that, lamentable as weie the cii'cum-
stances of their destruction, and scandalous as was the
waste of the property seized, there is little rea.'=ou to sup-
pose that any practical benefit would have flowed from
their continuance, whatever might have been the advautagea
of an honest and economical measure of reform, or even of ■>
transfer to other purposes on the principle of cy pres."
The negative evidence of the etTetene's of the older
orders supplied by their very small share in the counter-
Reformation, which lay virtually in the hands of the
Jesuits alone, is reinforced by the reports made by the
emissaries of the new company to their superiors, which
attest that the accusations of the German reformers again.^t
both the secular and regular clergy on the score of ign.^r-
ance and dissoluteness were only too well founded.
Accordingly several new societies were instituted during Later
the latter half of the 16th century, aiming at putting new societies
wine into the old bottles of the CarmeUtea, Cistercians,
Augustinians, Dominicans, and Benedictines ; but none of
them proved of much importance. A larger measure of
success attended some established on an active basis, such
as the Fathers of Christian Doctrine, a catechizing order
erected by Pins V. in 1571 ; two communities for tending
the siclc, one founded in Italy by Camillo de' Lolli in
1584, the other, the Brothers of Charity, by John of
God at Granada in 1538, but not formally sanctioned till'
1572; and still more [irosperity attended the Ursnline
Nuns, a comnumity chiefly devoted to the education of
young girls, founded at Brescia by Angela de' ilerici in
1537, and confirmed by Paul III. in 1544. Yet, \\ith the
single exception of the Jesuits, no new society could be said
to have laid hold in any degree of the popular mind, nor
were the attempts to revivify the elder bodies continued.
It remained for two newer still to rehabilitate the waning
respect for monachism of all kinds, and that by borrowing
one chief feature of the Jesuit organization, the abaiidon-
ment of that principle of isolation from the outer world
which lies at the root of true monachism. ^ Of these the
^ A full examinatiou of the ca^ against the n)Ouasteries T\ijl bo
found m Dixon, llistor!) </ Ou Cl.iiftli of Engloi'J, vol. i. pp. 321-
3S3.
Tlie number of houses suppressed and overthrown by the two Acts
of 1536 and 153S was as follow.:— 186 Beiiedicline houses, 173 Aujus-
tiuians, 101 Cistercians, 33 Dominican, Franciscan. Cermelite, and
Austin friaries, 32 rr.-vmonytratensiaus, 2S KuiRlits Hobi.iwHers,
25 Gilljcrtiucs. 20 Cluui.ics, 9 Carthusiani.. 3 Fontevnud. J
Miuoresscs, 2 Bonhoninies, 1 Brigittine ; total, 616. Their aggregate
revenues were valued at £142.9H, 12». 9cl. annu.illy.
' Soon after the Jesuits rose into note and popularity, .» very curioui
aud litlle kuowu ertcnsion of their iustitule was made in Flaudcn.
Two English la<lie^ acting with tho sympathy and counsel if not at
the recomniendatiou of F. Gcr.ird, rector of the Jesuit coUcu'o iit
\.\l'7P. fnuudcd a community which they named Jesuitesses, adoplins
MOIsACHISM
713
■first was t!ie Orator j, founded by Philip Neri in 155S, but
not approved by authority till 1577, and copied .'nde-
ptndently by Cardinal de BeiTille at Paris in IGll. There
Tvcre no vowi imposed on the members of this society
though they lived vmder rule, and they employed them-
selves in doing all kinds of clerical work under episcopal
supervision. The Italian house is chiefly celebrated as
having included the famous Cardinal Baronius amongst
its earliest recruits ; but the French one held a high place
in tlie religious revival of the 17th century, well-nigh
rivalling the Benedictines of St Maur in learning (with
such representatives as Simon, Thomassin, Morin, and
Malebranche), and the reformed Cistercians of Port-Royal
in piety, though sharing with the latter the reproach of
Jansenism. But the second was far more influential, and
has been fruitful ever since in the works of its copjTsts as
well as in ir,s own. It was the institute of the Sisters
of Charity, established by Vincent de Paul in 1634, on
the lines of the ancient community of the Hospitaller
Xuns of St Augustine, but with some remarkable modi-
fications, not only in respect of the vows, which were only
yearly and inward, but in the spirit of their discipline, as
forraidatcd in his own memorable words, — " Your convent
must be the houses of the sick ; your cell, the chamber of
suffering ; your chapel, the parish church ; your cloister,
the streets of the city, or the wards of the hospital; your
rule, the general vow of obedience ; your grille, the fear
of God; your veil to shut out the world, holy modesty."
The original scheme of Francis de Sales for the Nuns of
tlis Visitation, founded in 1610, was almost identical;
but the opposition was then far too strong, and he was
forced to m!.ke them a cloistered community. Vincent's
order of Mission Priests, more commonly known as Lazar-
ists, was also a successful and useful institute, though
not vying in the extent of its influence with the other,
which,* as has, been implied, has powerfully aflfected the
organization of many of the active communities which
jhave since been forme^. No religious body did more to
|enable French monachlsm to bear up against the general
obloquy it encountered during the 16th, 17th, and early
;18th centuries, — a temper on the part of the public due
to more than one cause. In the. first place, the wars of ^
religion had done much to harden and coarsen the "feelings
on both sides, and rigid adherence to the extreme positions
of Catholics or Huguenots, as the case might be, was set
far above any gentler and liigher ideas. Next, the monas-
teries of both sexes had. all but universally fallen into the
patronage of the crown (in virtue of .the concordat of
Bologna, between Pope Leo X. and Francis I.), and were
jobbed away as apanages for a dissolute nobility, who
bquandered the revenues, and suffered discipline to become
relaxed, often to the generation of serious scandals. This
malversation operated in two ways. It made the monas-
teries hard and bad landlords, grasping closely aU the
feudal privileges and monopolies which they continued to
enjoy, a proceeding which bore hard on the tenants and
labourers, so that the monks shared to the full the unpopu-
larity of the nobles (precisely as was the case in Germany,
during the Peasants' War of 1525) ; and the evil repute of
the nile aud orgnnizationof tlio famous compoay, and takisg the three
lisu.'\l rows, but, with a bold Jisi-eganl of precedent, not only omitting
the customary tow of inclosure, but actually sending the members of
the society out .is itinerant preachei-s. Their object w«3 to train a
body of emissaries for the Roman Catholic mission in lEngland, who
might obtain entrance and escape the incidence of the penal laws in a
nianLer impracticable for men. They had considerable success for a
time; and Jlrs Ward, their projector, obtained some degree of papal
approval, and becnme "mother-general" over more than 200 of these
I'.r.i.ale preachers in the various colleges of the society. But after an
existence of about eighty years it was suppressed by Pope Urban VIII
in 1630
the convents — of whose real c^iaracier we get at least one
trustworthy glimpse in the account of the abbey of ilau-
biiisson which Angelique Amauld reformed — came home
to all the Huguenots and their friends, because both before
and after the legal continuance of the edict of Nantes they
were used (according to a very early application of monastic
houses not yet obsolete) as prisons, where Huguenot womei?-
and girls were shut up in order to bring about their cor— r-
sion, forcibly if necessarj', but somehow in any case. And
there is evidence to show that the Huguenots resented thk
policy most bitterly, not only on polemical grounds, but bo-
cause they were firmly persuaded that the morals of ti^eir
wives, daughters, and sisters were in no less peril than their
faith iu such places. When to this sentiment is added the
hostility of the Jansenists to the school of opinion which
had persecuted them, razed their famous house of Port-
Royal, and literally flung the bones of its deceased member.^
to the dogs, it will be easy to judge how powerful were
the forces mustering for the overthrow of monachism, >nd
how little even such stem reforms as De Ranch's at La
Trappe, which has always had a marked attraction for
soldiers, could do towards abating the danger. Nor were-
there wanting public scandals and cases before the law-
courts which helped to fan the rising flames of hatred.'
Another cause which contributed much to the decay oS
discipline and of practical religion in monasteries of both
sexes was the custom which prevailed throughout the 16th,
17th, and 18th centuries, of disposing of the younger
members of poor but noble families in the cloister as a
safe and reputable provision, without any regard to the
vocation of these so dedicated, and merely because the
sum which sufficed to secure permanent admis-^ion was
much smaller than that necessary to purchase a commis-
sion or public office A)r a son, or to provide an adequate
dowry for a daughter.'' At the Revolution, the religious buijpn.-*-
houses, amounting (without reckoning various minor colleges *'"" pf
and dependent establishments) to 820 abbeys of men and ''""^l
255of women, with aggregate revenues of 95,000,000 livres, |„oDas>
were suppressed by the laws of 13th February 1790 and icriea.
18th August 1792. In Germany the storm had broken
somewhat earlier, if not quite so violently. The Thirty
Years' War had wrought much mischief to not .a few of the
religious houses, without taking into account the great
number Which had been destroyed in the territories of the
Protestant princes ; and when the death of Maria Theresa
in 1780 left her son Joseph II. free to act as he pleased,
he dissolved the Mendicant orders, and suppressed, in despit{
of the personal reiaonstrances of Pius VI., the greater numbei
of monasteries and convents in his dominions. In Italy,
despite the multiplication of new institutes, the process
of decay continued throughout the 17th century, and one
most remarkable testimony to the fact appears in the
report. of the Venetian ambassadors at Rome in 1650 to
their government of on interview they had \rith Pope
Alexander VIL
^ One of these is interesting, as settling a point which has bean
often disputed, — the existence of those mouastic dungeons known by
the name of *' in-pace," f.amiliar to the readers of Marmion. It is the
condemnation of the abbot of Clnin-aui by the parle:nent of Paris in.
1763 to a fine of 40,000 crowns for causing the death of a prisoner in
an "in-pace." «
* This worked mnch evil in France, but produced perhaps even
greater mischief in Germany, where what were styled ** Noble Abbej-s"
were not uncommon, entrance to which, save in the inferior capacity
of lay-members, was barred against all who could not prove patrician
descent and a certain number of armorial qnartcrings. A relic of this
survives in a few secular Stijlungen (Protestant and Catholic) for noble
canonesses in Germany; aud the notion was at any rate as respectable
as that which holds good in some communities even now, where women
who can pay a certain sum at entrance are admitted as choir-sisters,
while those who cannot do ao must accept the humblor position of lay-
sisters.
XVX — 9<»
714
MOi-^iiCHISM
"The Pontiff . . . began by saying that for some time past the
Apostolic See, considering not the abundance only, but the super-
fiuity of religious institutes, had become convinced that some of
them, degenerating from the first design of their founders, had
lapsed into a total relaxation of discipline, and that it was just as
advisable for the church as for the laity to adoj.t the expedients
used by wise husbandmen when they see that the multitude of
branches has impoverished their vines instead of making them more
fruitful. That a beginning had been made in that matter by sup-
pressing some orders; but this was not enough A great
number of very small convents had been supj.ressed, . . . and
it was proposed to continue the work by proceeding to the final
abolition of certain others which, by their licentious mode of life,
filled the world with scandal and murmurs. . . . Tliat he proceeded
slowly, because he desired, in a matter of so much importance, to
obtain the good-will of the secular princes. . . ." The remarks
closed with a recommendation to the republic of Venice to suppress
the canons of San Spirito and the Crucifcti in their city, and to
apply their revenues towards defraying the cost of the war in
Candia. (Ranke, Die Rom. Pdpate, App. Ko. 129.)
But the policy thus indicated was not carried out Ijy
Alexander VII.'s successors, and there is evidence that
things did not mend as time went on. The emperor
Francis I., in his character of grand-dul;e of Tuscany,
caused an edict to be published at Florence in 17.51,
forbidding tlie clergy to acquire property in mortmain,
and is.sued together with it a paper of instructions pointing
out the grave social disadvantages of enriching artificial
families, such as convents, colleges, and the like, at the ex-
pense of natural families. And the menace implied in these
documents was carried into operation by the suppression
of several convents of nuns, for which the reluctant con-
sent of the pope (Benedict XIV.) was extorted. When
Francis died in 1765, and wa.9 succeeded in Tuscany by
his brother Peter Leopold, the latter began his reign with
what may be styled a formal act of war against the Roman
Curia, by declaring the bull In Ca'na Domini null and
void in Tuscan}', and forbidding its recognition 'or publi-
cation there. At once he was beset with appeals from
priests and nuns, calling his attention to several grave
abuses in the church, and notably to moral scandals of the
most serious kind in the convents of nuns, especially those
under the direction of the Dominicans, accusations which
were fortified with full details of time and place. The
result was that Leopold caused a scheme of ecclesiastical
reform to be drawn up in 1770, containing stringent
enactments for the abatement of nionachism, for the
suppression of all small convents of mendicants, and for
the exclusion of monks and friars from the direction of
nunneries, which were to be subject in all spiritual
matters to the ordinaries only. And the Jansenist bi,shop
of Pistoia and Prato, Scipio de' Ricci, upon entering on
bis diocese in 1780, at once began to inquire into the
scandals which raged in the Dominican nunneries of his
jurisdiction, especially in Pistoia,' the result being that he
excommunicated the Dominican friars, and prohibited
them from officiating. The pope at that time was Pius
VL, an ardent devotee, warmly in favour of mona-
chism generally, and of the lately suppressed Jesuits in
particular, so that he took up the cause of the friars
(though their evil rejmte Lad prevailed for 150 years),
and issued a brief of censure against Ricci. He laid
it before the grand-duke, -who wrote a strong remon-
strance, accompanied with proofs furnished by Ricci, and
informed the pope that unless the brief were promptly
withdrawn, and the convents obliged to submit to
the ordinary's jurisdiction, he would hi.uself reform at
bis own discretion every religious hou.se in Tuscany.
Accordingly, thg brief was retracted, and Ricci was given
full liberty to repress the disorders complained of. There
is not any similar evidence forthcoming as to the condition
' As to which documentarv evidence will bo found in the Appendij
loDe Potter's Life o/ Scipio de' Ricci.
of the mona.steries in other parts of Italy; but Tuscany is
likely, from local cause.s, to have been above, rather than
below, the average moral level. Against this general
tendency to monastic decay may be set the foundation of
the Passionists in 1725, and of the Redemptf,ri.st3 or
Liguorians in 1732; but the.se two institutes, though piou-s
and respectaVjIe, have never exerted much influence.
There is little to chronicle in regard to the later annals
of monachism in Spain and Portugah Peter of Alcantara,
as reformer of the Franciscans of the latter country in
the middle of the ICth century, and his more famous
contemporary, Teresa, as reformer of the Carmelites in
Spain, are eminent figures in the annals of their time; but
they cannot be said to have produced any permanent
effect on the fortunes and tone of their several institutes,
far less upon the common life in general. The stamping
out of all varieties of opinion, at any rate in respect of
outward expression, by the Inquisition in the Peninsula
makes the evidence scanty and vague; but the fact that
Portugal took the lead in 1759 in striking at the Jesuit.?,
then the most eminent and powerful of the orders, thou"h
far surpassed in mere wealth and numbers throughout
Western Europe by the Franciscans, and that its jiolicy in
this respect was quickly followed by Sjiain, attests the
growth of a hostile feeling by no means likely to have
been limited to the great company. In fact, if popular
rhymes and proverbs may be trusted, the charges current
against the religious orders in Sjiain do ^ot seem to have
differed from those alleged elsewhere, whatever may have
been the amount of truth in them. And the testimony of
Blanco White, always to be trusted on matters within hxi
experience, is decidedly adverse.
The terrible crash of the French Revolution, which
affected, directly or indirectly, every country in Europe,
was not least influential in its incidence on monachism.
On the one hand, the actual destruction which it brought
u]jon the religious houses of France was adopted as part of
the revolutionary programme in all countries where such
institutions were still intact ; and, on the other, there was a
considerable measure of improvement brought a'oout in
not a few places by the fear of public opinion, while the
new institutes which continued to spring up were all but
invariably active, both founders and the sanctioning
authorities recognizing that any society seeking to make
its footing good must needs first prove its caiiacity for
practical usefulness. In France itself the laws which
abolished all religious communities were relaxed by con-
nivance in favour of the Sisters of Charity even under
the Terror and the Directory; while in 1801 a decree of
the Consular Government, issued by the Minister of the
Interior, authorized Citizeness Dukau, former superior of
that society, to revive it by taking young women to train
for hosjjital work ; and various other active communities
were restored by ^Napoleon in 1807. Further revivals
took place at the F.c .(oration, the most celebrated of
which was the Dominican, owing to the talents and elo-
quence of Lacordaira and the group he gathered rcund
him; but Benedictine.?, Carthusian.s, Trapj.ists, and olher
societies of the older typo were not slow to avail them-
selves of the opportunity to return and to found anew,
amidst a poverty which recalls the original institution,
their abbeys and priories. But they met with little favour
under the Orlcanist monarchy, and the Second Empire was
their time of most security and jirogress. Since its fall,
they have again been actively discouraged by a strong
party in the Republic and their po.sition remains j'rc-
carious. France has bopa further, the chief seat of the
many new societies founded for some especial department
of charitable work, the most characteristic example of
which is perhaps that of the Little Sisters of the Poor,
iVI O N A C H -I a M
715
•vho nouse ana tenu aged invalids. As a broad ge leial
rule, nearly every pott-]leformation institute is styled, not
an "Order," but a "Congregation"; but the only dis-
dnction which can be drawn between these two names
is that "order" is the wider, and may include several
congregations \vithin itself (as the Benedictine order,
for example, includes the congregations of Cluny and
of St Maur), while a "congregation" is a simple unit,
complete in itself, and neither dependent on another
institute nor possci.sed of dependent varieties of its own.
Another distinction drawn between the elder and younger
societies is that the former are said to make "solemn
vows," the latter only "simple vows." The difference
here is not in the matter of the vows, which are usually
the same in all cases, nor even in the ceremonies attending
their utterance, which may also be alike, but in the
superior binding efficacy of the solemn vows in Roman
canon law, which rules that they so bind the member to
his society, and the society to each member, that neither
can sever the connexion, so that only the pope can dissolve
it, and that in rare and exceptional cases alone. And it
may be added that the term "religious" is restricted in
the Latin Church to communities whose institute has been
formally approved by the Roman see, and whose vows
are for life, and not merely renewable, — a principle which
excludes the Sisters of Charity, for example, from the use
of this title. By the laws of France, and of some other
countries, life-vows are invalid and even prohibited, but
when they make part of the original institute, such dis-
approval by the civil power is not held to reduce them to
the canonical level of temporary vows.
Returning to the history of Western monachism, the
fall of the religious houses in Spain dates from the law of
21st June 1835, which suppressed nine hundred monasteries
at a blow; and the remainder had but a short respite, as
they were dissolved on 11th October of the same year. In
Portugal, where a bias against the Roman Curia has been a
traditional part of patriotism ever since the revolution of
1640, when the pope sided with Spain against the house
of Braganza, there v.-as little feeling to protect the
monasteries when it happened that the cro\vn wanted
their possessions, and they were all suppressed by the
decree of 28th May 1834. No European country had so
many religious houses as Portugal in proportion to its
population and area, and the number of the foundations
dissolved in 1834 exceeded 500. In Switzerland, a con-
siderable measure of suppression followed the war of the
Sondcrbund in 1847 ; while in Italy, the last country
where monachism had remained almost unmolested, an Act
was passed in the Sardinian Parliament on 7th July 186G
for the suppression of monasteries within the Piedmontese
ilominions, and for the confiscation of their properly.
The measure was extended to the whole of Italy after the
unification of the kingdom ; the orders were expropriated
in 1873 ; their bouses were declared national property, and
were put to secular tises, no exception being made in
favour of San JIarco at Florence, ui Assisi. ot Vallom:
brosa, or even of Monte Cassino itself.^
On the other hand, several Roman Catholic societies'
have attained considerable success in the United States
and Canada, thus in some degree recovering for the
principle they represent part at least of the ground lost in
Europe ; while in three religious communions outside the
pale of the Latin obedience — the Evangelicals of Germany,
the Reformed of France, and the Church of England — the
organization of women for charitable and religious work
on the lines of various old institutes has been actively
carried out. The Deaconesses of K.aiserswerth, founded
by Pastor Fliedner in 1836, derive part of their rule, and
even of their dress, from the Dames de St Augustine,
themselves lineal descendants of the first Hospitallers of
the crusades, and have ramified into several countries ;
the Strasburg and Miihlhausen Deaconesses derive theirs
partly from the Flemish Beguines and partly from some
points in the Moravian organization, itself handed d^ivn
from those seceding Franciscans to whom the Uniias
Fratrum really owes its origin ; while the various Ajiglican
communities, of which there are several, have borrowed
freely from different sources, according to the preference
and knowledge of each founder. Some attempts at
reviving the common life for men also have likewise been
made, but none on any large scale ; only one has as yet
exhibited any signs of vitality, a preaching ord«r at
Cowley, near Oxford, which has obtained some footing in
England, and has even been able to spread to America.
bibliography. — The bibliography of Jtonachism is excessively
copious, and it is impracticable to indicate more than a few of the
most important and trustworthy books. General: — Hospiuianus,
Dc Monachis LihH Sex (Geneva, 1659), bitterly hostile, but a copious
and trustworthy record of facts ; Helyot, Hisloire dcs Ordrcs Iteli-
gieux (8- vols., Taris, 171'i-1721), and again (as Diclionnain dcs
Ordres Rcligicux), with continuation by Badiche (4 vols., Paris,
Jligne, 1860), — this book has itself a copious catalogue of works
on its subject prefixed ; Alteserra, AsccticOn, sivc Origimtvi I^ci
Mona^iicea Libri Decern (Paris, 1674) ; Holstenius, Codex Hc'jularum
(3 vols., Rome, 1661); Slontalembert, Moines d' Occidtnt (7 vols., Paris,
1860-1877) ; Dugdale, Monasticon Anglicanum (edited by Caley,
Ellis, and Bandinel, 8 vols., London, 1846) ; Rosweyde, Vilm Patrum
(Lyons, 1617). .Special :^— Benedictines — llabillon, Aeta SS. Ordi-
nis S. Bcncdidi (9 vols., Venice, 1733) ; Cluniacs— Harrier, Biblio-
Iheca Cluniacensis, (Paris, 1614); Cistercians — Gaillardin, Les I'rap-
pisks (Paris, 1844) ; Besoigne, Hisloire de V Ahhaije de Porl-Hoyal
(8 vols., Cologne, 1752-56); Dominicans — Touron, Sislcire dcs
Horiivies Illusires dc VOrdre dc Saint Dominique (6 vols., Paris,
1743-49) ; Franciscans— Sedulius, Hisloria, ScrajMca (Antwerp,
1613) ; Wadding, Annates Uinorum (20 vols., Kome, 1731-94).
(R. F. L.)
* The total number of monasteries, &c., suppressed in Italy down to
the close of 1882 was 2255, involving an enormous displacement of
property and dispersion of inmates. And yet there is some reason to
think that the state did but do roughly and harshly what the church
should have done more gradually aud wisely ; for the judgment passed
on the dissolution by Pius IX. himself, in speaking to an English
Roman Catholic bishop, was : "It was the devil's work ; but the good
God will turn it into a blessing, since their destruction was the only
reform possible to them." (Cited by Rev; R. R. Suffield in Modem
JUview, voL iL p. 359, April 1881.)
Chkonological Table of Monastic FotnrDATioNS.
The religious communities which have been formed at various times in the Western Church amount to many hundreds, and receive frcsli
accessiona almost yearly, while some among them have been suppressed, absorbed, or suffered to die out. No oBicial list of those actually
in existence and recognized by authority is published ; it is thus impracticable to enumerate them accurately, especially as many of
them are only local varieties or branches of iden tical rules and institutes, aud there are not a few cases where a once celebrated and powerful
order has practically disappeared from view, though, as still lingering in one or two houses, not definitely extinct. The following table,
however, gives the more remarkable foundations in chronological order, some of the earlier dates being only approximate, and even a few
later ones uncertiin, for the historians oftei. vary as to the exact year, sometimes giving that of the first attempt at oiganization, and
sometimes that of the final approval by authority.
Date.
Name.
Founrlcr. 1 Place.
Date.
Name.
Founder.
Place.
250
320
Monka of the niebaid
Paul the Hermit 1 Upper Egypt.
Pachomius 1 Tnhenure, in the
Nile.
Basil the Great j Mataza, Pontus.
395
400
Aastin Canons (original) . .
Accemeti, or - BleeplesB
Monks
A tnicifnft
Hippo Regius,
Africa.
Mesopotamia.
716
MONACHliSM
Date.
Name.
Founder.
Place.
Date.
Name.
Founder.
Pla«. j
420
529
540-6V0
663
600
641
?C0
910
1012
10S9
losim
1074
10S4
loss
KBS
iioom
llOO
1104
1118
nioa)
iico
U40
1143
115i)
1156
115S
1102
1170
1179
1191
1196(7)
1197
1193
1200(?)
1203
1209
1212
1212
1214
1214(?)
1215
1213
1218
12ai
1223
1231
1211
1251
1271
1290
1298
1313
1S50(?)
1355
1363
1366
130S<?)
1373
1S73-77
1376
1380
1390(7)
l;i05
1403
1408
1425
14.9
Honoratus of Arlea .
Benedict of Nursia**?
Dubric, Illtut, David
Columba
Colurabanus
Itubcrga, wife of Pip-
pin of Landen
I. of Lerins,
•France.
Monte Cassino,
lUly.
Wales.
lona, Scotland.
Anegray, France.
Nivelles, Flan-
ders.
Metz.
Cluny, France.
CamaldoU, Italy.
Vallombrosa,
Tuscany.
Avignon CO-
Mount aioret,
Limoges.
Near Grenoble.
Vienne, Dau-
phine.
Molesme, Bur-
gundy.
Jerusalem (7).
Fontevraud, Poi-
tiers.
Jerusalem.
Jerusalem.
Jerusalem.
Pr^raontT6, Pi-
cardy.
La Trappe,
France.
Sempringhsm,
Lincolnshire.
St Julian, Ciudad
Rodrigo.
Pesoara, Italy.
Calatrava, Spain,
Evora, Portugal.
CompostcUa,
Gaiicia.
Liege.
Acre, SjTie-
Milan.
Meaux, Paris.
MontpelUer,
France.
Germany.
Assisl.
Mount Carrael,
Palestine.
Assisi. Italy.
ChaumoniT
France.
Clair-Lieu, Bel-
gium.
Cesena, Italy.
Bologna. '
Buda-Pesth,
Barcelona.
Assisi.
Florence.
Osimo, Italy.
Mantua.
Morseilies.
Sulmona, Italy,
France and Flan-
ders.
Paris.
Siena (?), Italy.
Aix-la-ChapelIe<?)
Siena.
Wadstcna,
Sweden.
Bruliano, Italy.
Villaescuda,
Caatile.
Pisa.
Deventer,
Holland.
Piesole, Italy.
Toledo.
Home.
Padua.
niceto, Siena.
Xear Toledo.
AbhpyofStMat-
thics, Treves.
1431
1433(7)
'1433
1435
1443
1414
■ 1453
14S4
1493
1503
1524
1525
1531
1602
1533
1531
1537
1533
1551(?)
1553
1568
1571
1577
1578
1579
1584
1588
15S8
1594
1595
1596
1608
1609
1610
1611
1611
1615
1617
iei7
1018
1621
1624
1624
1624
1625
1629
1633
1639
l&iO
1641
1641
1643
1643
16-i5
1050
1653
.lO^
1660
1661
1063
1673
1670
1034
1680
Mitigated Carmelites, or
"BiUettes"
Congregation of St Ambrose
ad Nemua
Pope EugenlUfl IV. . .
(?)
Rome (?).
Benedictines, or Black
Monks
Frances of Rome
Francis de Paola . . . .
Nicolas Rclin, chan-
cellor of Burgundy
Grsgorio Rocclii
Bishop de Boppart . .
Pope Innocent VIIL'
Jean Tisscrand
Queen Jeanncdc Valois
Giovanni Pietro Ca-
r?.fld(Pop£'PaulIV.)
Matteo di Bassi
GirolamoEmiliani
(1) r-
Giacopo Antonio Mo-
rigia
Ignatius Loyola
Angela de' Merici
John of God
An Englishwoman,
named Ward
Philip Neri
Mintms, or Hermits of St
Francis
Daughters of St Martha
(Hospitallers)
Augustins of the Lombard
Congregation
Monka of LuseuU
Nuns (later Canonesses) of
Nivelies
Beaune, Prance.
Benedictines of Cltmy
Order of CamaldoU
Order of VallombroM
Austin or Black Canons . .
Order of Gi-ammont
Metz. ;
John Gualbert
Bamabites, or Clerks Regu-
lar
Rome.
Bourges, Fnuic«v
Bru::
Capu';hin3, or Reformed
Clerks-itegular of St Ma-
jolus of Pavia, or "So-
maschi "
Recollects, or Strict Fran-
ciscans
Bamabiu's of St Paul
Italy.
Order of 3t .AJithonv of
Vienna
Pisa.'
Pobsrt
Pavia.
Crucireri ^suppressed, 1,658)
Order of Fontevraud
Knights Hospitallers of St
JoLm
TBmplai-3 (sappres'jecl in
1S13>
Knighta of St Laaarua
Canons Rcgtuir of Pie-
montrd
Robert d'^Vrbrissel
Gerard (Raymond du
piiy, first Grand
Master)
Hugh de Payens
C?) ...-
Norbert >.....
Rotrou II., count of
Perche
Gilbert of Sempring-
ham
Suero, and Gomez, de
Barrientos
William dc Malavol . .
SnnchoIII., of Castile
Alfonso I., of Portugal
Ferdinand II., of Leon
Bega, or Lambert le
B^guo
HeiiiTich Walpot
Spain (?).
Milan.
Paris.
Brescia, Italy.
Granada.
Flanders.
Brothers of Charity
Jesuitesses (suppressed.
1631)
Discalced Carmelites
Fathei-s of Christian Doc-
trine
A Vila. Spain.
Pope Pins V
Jean de la Barrii-re . .
Carlo Borromeo
Pope Gregory XIH."..
Camillc de* LeUi ....
Agostino Adorno ....
Thomas d'Aiidrada
(Thomas de Jesus)
Vincent Blussitrt
Juan Baptista Garcias
Madeleine d'Escou-
bleau de Sourdia
Jean Michaelis
Knights of Alcantara
Hennit9 of St William, or
White-Mantlea
Knights of Calatrara
Knights of St Bennetof Aviz
Knights of Santiago cf the
Sword
Oblates of St Ambrose
Latin Monks of St Basil . .
Clerks Regular, Ministers
of the Sick
France.
MUan.
Rome.
Rome.
Discalced Aogustinians . .
Conjjrcgation of Picpos
Discalced Trinitarians .. ..
Notre Dame de St Paul . . .
Jacobins, or Reformed Do-
English Institute of B. V.
Mary
Nuns of the Visitation
French Ursulines
French Oratorians
Canons Regular of St
Saviour
Hospitaller Nuns of St
Charles
Pauline Congregation of
the Mother of God
Talavera.
Teutonic Knights
Hiimiliati (suppressed, 1570)
Franconville- ,
sous-bois. Parte.
Vul de FeBu«
John do Matha and
Fe'.ixvde Valois
Guy of Montpellier . .
Spain.
Knights Hospitallers of the
Holy Spirit
Penitents of St Mary Mag-
dalene
St Paul, Praace.
Paris.
Francis Bomardone . .
Albert, titular patri-
arch of Jerusalem
Francis and Clara
William cf Paris
Theodore da Celles . .
Giovanni Bono
Dominic Guzman ....
Eusebius, archbp. of
Strlgonia
Jayme I., of Aragon..
Jeanne Fran<;oi3e de
Chautal
Marie Lhuillier
Cardinal de BeruUe . .
Fourrier de Matain-
court
Joseph Calasanza
Antoinette d'Orlcans
Didierdc la Cour
Simonc Gauguin '
(Mother Frances of
the Cross)
Vincent de Paul
Marie Elizabeth de
RjiTifain
Nuns of St Clare
Onler of Val-des-Ecoliers . .
Canoas Regular of the Holy
Cross
Hermits of St Augustine ..
Paris.
Paris.
Lorraine-
Nancy.
Rome,
Hermits of St Paul
Order of St Mary of Merey,
or Mercedarians
Franciscan TertiarJes
Poitiers.
Congregation of Benedic-
tines of St Mftur
Hospitaller Nuns of the
Charity of Our Lady ....
Lftzarists
Nuns of Our Lady of Refuge
Religieusea de la Croix
Verdun, Ftanoe.
Paris.
Buonfiglio Monaldi . .
Sylvester de' Gozzolint
Alberto Spinola
Innocent IV
Pictro Moi-one (Pope
Celestine V.)
Canons Ketnilar of St Mark
Austin Brothers of Peni-
Paris. >
Nancy.
Grey Sisters, (Hospitallers)
HoBpiUller^ of the Chaiity
of our Ludy
Vincent de Paul and
Louise Legras
Antoine" YA'an and
Madeleine Martin
Antoine Lequien
Bartholomew Holi-
h.iuscr
Madeleine Limy
Paris.
Guy de Jolnvflle
Bernardo Tolomel of
Sieua
(?)
Ail, Proyence. \
Sisters of the Blessed Sacra-
ment
Bartholomites. or Clerks
Secular of Common Life
Kuns of the Good Shepherd
Order of Our Lady of Char-
ity and Kelugo
Kudist:-,, or Mi^ibicn Priests
DftUi^lit^rs of Providence . .
Marseilles.
CcUitea, or Alexlan Brothers
Salzburg.
Giovanni Oolombini .,
Bridget of Sweden
Bridget of Sweden
Paoletto de Foligno . .
Pedro Fcrrando Pecha
do Guadalajara
Pietro Gambacorti or
Gambacurts
Gerard Qroot
Carlo de Montograneli
Maria Garcias .,.,*....
Bartolommco Colon na
Ludovico Barbo
Stephen Ciooi of Siena
Martin Vaam
Joliann Rodius
Caen, Franca. -^
Eri^ittino Nuns, or Order
of St Saviour
Brigittine Knights
0>)ijcrvants, or Franciscans
of the Strict Observance
IlioTonymitc Monks
Hermits of St Jerome
Brothers of Common Life. .
Fcsnlan Mendicants of St
Jerome (suppressed, 1008)
Hieronymlte Nuns . . ;
Con/fregation ofthc Late ran
C >ngregation of St Juatina,
r.r iieform of Moute
Cassino
Canons Regular of St
Saviour
Often.
Madame de Polalllon
J»an Jacques Olier .,
Henri ilaupas du
Tour
Catherine do hunt-
(Mcchtildo du St-
Pierre de Bdtaucoart
Ange Le Proust
PireVachct
Armand do RancA
Nicolas Barr6
Madame Morel
Marie Poussopin
Mndnmrde Maintcnon
and Louis XIV.
Paris.
Sisters of St Joseph
Benedictine Nuns of Per-
petual Adoration
LePuyenVelay,^
France.
Paris.
Hospitaller Nuns of St
Thomas of VillaJlova
Union Chnitlenno
Reformed Trappista
Brothers and Sisters of the
Child Jesns
Daughters of Providence . .
Sisters of the Presentation
Aiiieric*.
Laiiiballe,
France.
Charotine, Paris.
La Trappe.
Paris.
Ctnrlevllle,
Franco.
SainvilJc, Franc*.
Order of Bursfeld, or Ger-
man Benudictiac Reform
M O N — M 0 N
717
ratn.
Name. 1 Foaoder.
Place.
Date.
Name. Foundei.
Plate.
1680
Daughters of the Good
Shepherd
Madame de Combe . .
Paris.
1842
Deaconesses of St Loup
(Swiss Refd.)
M. Germond
Echellenc,
1704
Sisters of Charity of St Paid
the Apostle
Louis Chanvet
Lev6vlUe-U-Che-
nard, Prance.
1848
Notro Dame de Sion
PP. Theodore and M.
A. Ratisbonne
Paris.
1712
congregation of the Good
Saviour
Religious of Most Blessed
Elizabeth de SurviUe
St - Lo, Nor-
mandy.
Bousseauz-le-
1846
Society of the Holy Child
Jesus
Society of Holy Trinity of
Devonport (Angl.)
Cornelia Connelly
Derby, England.
1718
P6ro VIgne
1847.
Priscilla Lvdia Sellon
Plymouth.
Sacrament
Roy, France.
1716
Daughters of Wifidom
Marie Louise Trichet
and Grignon de
U RocheUe.
1848
Siatera of the Poor Child
Jesus
Clara Fey
Aii-la-Chfipdle.
Montfort
1840
Poor Handmaids of Jesus
Katharina Ka<ip&r . . .
Deimbach, Ger-
1725
1732
Paaaloniats
Panl of the Cross
Alfonso de' liguori ..
Rome.
Scala, Italy.
1849
Christ
Bisters of St Mary the
Miss Lockhart
many.
Wantage, Berks.
Redcmptorlsts, or Ligu-
orlans
Virgin (Angl.)
1786
Society of the ClirlstJan
Antoine Sylveotre
Fontenellea,
1860
SUters of the Most Holy
F. Gaudentiua
Manchester.
Retreat
Receveur
France.
Cross and Passion
1800
Ladles of the Sacred Heart
Madame Barat
Amiena.
1851
Sisters of Nazareth
Cardinal Wiseman
Hammersmith,
1801
Dames de St Andri
Seraphine Hauvarlet
Toumay, Bel-
I-oudou,
gium.
1851
Sisterhood of All Saints
Rev. W. Upton
London.
1815
1815
Mariat Fathers
Jean C. M. CkjUh ....
M. de Mazenod
^^
1853
(Angl.)
French Oratorians (revived)
Richard*
Abb6 Pfitctot
Paris.
Obbtes of Mary Imnuca-
18l«
Ute
Sisters of Jesaa and Mai;y. .
P6re Coludie
Fourvlires,
1862
Deaconesses of Riehen
(Swiss Refd.)
M. Spittler
near Basel.
Lyons.
1864
Society of St John Baptist
Hon. Mrs, Charles
Clewer,Wiu'l6oi.
181T
Marlst Brothera
Abbe Champagiiat . .
Lyoas.
(Angl.)
Monsell
1620
Sisters of Notre Damo
Julie Eilliart
Amiens.
1855
Nursing Sisters of St Mar-
Dr John Mason Neale
East Gi instead,
1820
Sceurs de TEsp^rance
Brothers of Christian In-
Abb6Noaines
Bordeaux.
garet (Angl.)
BoBsei.
1822
Abb^ Lamennals . . .
St Brieuc, France
1856
Helpers of the Holv Souls
Deaconesses (Angl.)
Eugenie Suret
Paris.
struction
1861
Rev. T. Pelham Dale
London.
1832
Faithful Companions of
Jesus
Madame d'Houet ....
Amiens.
and Elizabeth Cathp-
rine Ferard
1822
Society of Nazareth
Pierre Roger
Slontmirall,
Franco.
1861
Sisterhood of St Peter
(Angl.)
Rosamira Lancaster . .
Brompton,
London.
1824
Sisters of Bon Secours
Madame de M<5ntale . .
Paris.
1861
Congregation of the Finding
Mary Lefevrc
London (now
■ 1824
182T
1828
Marist Sisters
Jean Claude Colin
Catherine McAuley ..
Abbe Debrabant ....
Belley, France.
Dublin.
Doual, Prance.
1S&4
of Jesus in the Temple
Little Sisters of tlic As-
Angnstinions of the
Clifton Wood,
Bristol).
Paris,
Sisters of Mercy
Jji Sainte Uniou des Sacrts
Coeurs
sumption
Assumption
1620
Institute of Charity, or
Antonio Eosmini-Ser-
Monte Calvario,
1805
Sisterhood of St Mary
Rev. Dr Morgan Dix. .
New York.
Roamintan Fathers
bati
Italy.
(Angl.)
Mission Priests of St John
1833
School SistetB of Notro
Bishop Michael Wiss-
Nuremberg
1865
Rev. R. M. Benson . .
Co-wley St John,
Dame
mann
Bavaria.
the Evangelist (Angl.)
Oxford,
1833
Daughters of the Cross
Canon J. G. Habets
and Jeanne Haze
Li^ge.
1866
Servants of the Sacred
Heart of Jesus
P. Peter Victor Braun
Paris.
1836
Deaconesses (Lutheran) . .
Theodor FUedner ....
Kaisers werth,
DOsseldorf.
Bruges, Belgium.
1866
Sister£i of Bethany (Angl.)
Etheldreda A. Benett
Pentonville,
London.
New York.
1837
Xaverlan Brothers
Theodore Ryken
1860
Sisterhood of the Good
Bishop Horatio Potter
1840
Deaconesses (FreDch Re- M. Vei-meilaud MdUe.
Paris.
Shepherd (Angl.)
formed) Malvesin
1870
Sisters of the Church
Emily AyckbowQ
Kilbum, London.
I&IO
Little Sisters of the Poor . . Abb6 le PaiUeur
St Malo.
(Angl.)
1842
Deaconesses of Strasburg , Pastor Harter
(Luth.) 1
Strasburg.
1870
Little Company of Mary . .
MaryPotter
Hyson Green,
NoHingham.
MONACO (French Monegue), the smallest of the soTe-
reign principalities of Europe, with an area of 8 '34 square
miles, a population (1878) of 7049, and an army of 72
men, is situated on the coast of the Mediterranean, 9 miles
east of Nice, and bounded on all sides by the French
department of the Maritime Alps. Previous to 1861,
when the communes of Mentone (Menton) and Roccabnina
(Roquebrun) were sold to France for 4,000,000 francs, the
area was about a third larger ; but the population, which
with those portions again included would now be 15,000,
was only about 8000. Monaco has long had the reputa-
tion of being one of the most beautiful and sheltered
spots on all the Franco-Italian coast : non Coma in ilium
Jus hahet aut Zephyi-ua ; solus sua littora turbat Circius,
said Lucan ; and a luxuriant growth of aloes and prickly
pears (introduced in 1537), palm-trees, eucalyptus, lemon-
trees, and geraniums gives a warmer colour to the scene
than Lucan can have known. The town occupies the level
sununit of a rocky headland, rising about 195 feet from
the shore, and still surrounded with ramparts. Though
largely modernized, the palace is a fine specimen of Re-
naissance architecture; the new "cathedral" (French Re-
naissance style), the new church of St Charles, and the
museimi may also be mentioned. Behind the rock, between
Mont Tete de Chien and Mont de la Justice, the high
grounds rise towards Turbie, the village on the hill which
takes its name from the tropsea with which Augustus
marked the boundary between Gaul and Italy. On the
eastern side lies the little port or bay of Monaco ; along
the lower ground at the head of the bay stretches the vil-
lage of Coudamine with orange-gardens, manufactures of
perfumes and liqueurs, and the chapel of Ste Devote, the
patron saint of Monaco : farther to the east, on the rocky
slopes of the Sp^lagues (Speluncje) are grouped the various
buildings of the Casino of Monte Carlo and the numerous
villas and hotels which it has called into existence. Previous
to 1828 the Spelugues were mere barren rocks ; but after
MONACO'*^:— -T^saartei.
Plan of Monaco.
they were traversed by the new road to Mentone, Count Eoy
caused them to be covered with soil by Italian convicts ;
and since 1858, when the first stone of the Casino was
laid, the process of artificial embellishment has been carried
718
M O J^— i\i O iS
out on the most magnificent scale. The gaming establish-
ment is now in the hands of a joint-stock company with a
capital of 15,000,000 francs. None of the inhabitants of
Monaco have access to the tables ; and their interest in the
maintenance of the status quo is secured by their complete
exemption from taxation, and the large prices paid for
their lands. GamMing-tables were set up at Monaco in
1836; but it was not till 1860, when M. Blanc, expelled
from Homburg, took possession of the place, that Monte
Cailo began to be famous.
A templo of Heracles Moutecus was built on the Monaco head-
land at a veiy early date, probably by the Greeks of Massilia.
MoncBci Poitus or Portus Herculia is frequently mentioned by the
later Latin writers. From the 10th century the place was associated
with the Grimaldi, a poweiful Genoese familj who held high offices
under the republic and the emperors ; but not till a much later
date did it become their permanenf. possession and residence. In
the bejinning of the 14th century it was notoi-ious for its piracies.
Charles I. (a man of considerable maik, who, ifter doing great ser-
vice bj sea and land to 'Philip of Valois in his English wars, was
severely wounded at Ciecy) purchased Meutone and Roccabruca, and
bought up the clainia of the Spinola to llonaco. The princes of
Monaco continued true to France tdl 1524, when Augustin Grimaldi
threw iii his lot with Charles V. Houore I., Augustin's successor,
was made marquis of Campagna and count of Canosa, and people
as well r.s lulers were accorded vaiious importaut privileges. The
right to exact toll from vessels passing the port coiitijiued to be
exercised till the close of the 18th century. Honore II., who re-
newed the alliance with France iu 1G41, was compensated for the
loss of Canosa, &c., with the duchy and peerage of Valentinois and
various lesser lordshins ; and duke of Valentinois long continued
to be the titlS of the lieir-apparcnt of the principality. The Na-
tional Convention annexed the principality to France iu 1793 ;
restored to the Goyon Grimaldis by the Treaty of Paris in 1814, it
w.a3 placed by that of Vienna under the protection of Sardiuia.
King Albert of Sardinia took the opportunity of disturbances that
occurred in 1848 to annex ilentone and Roecabruna ; but this
liigh-handed proceeding was condemned by the protocol of 1856,
and Charles III. (born 1818) entered upon his full rights. With
the transference of Nice to Fiance in 1860 the principality passed
again under French protection.
See Charles de Venasque's. Geiicaloglca H historica Grimaldis gerttis arior
frtally the work of HoDoie 11.).
MONAGHAN, an inland county of Ireland in the
province of Ulster, is bounded E. by 'Armagh, S.E. by
Louth, S. by Meath, S.W. by Cavan, W. by Fermanagh,
and N. by Tyrone. The area is 318,806 acres, or 498 .sq.
miles. The north-western part of the county is included
in the great central plain of Ireland ; but in the south-east
there is an uprising of .Lower Silurian rocks. The surface is
irregular, although none of the hills are of great elevation.
The principal range is that of Slievebeagh, a rugged and
barren tract extending into Fermanagh, its highest summit
being 1254 feet above sea-level. Formerly much of the
country was under forest, but it is now very bare of trees,
except in the many demesnes of the nobility and gentry.
The scenery is redeemed from monotony by the large num-
ber of small lakes and streams. The lakes number in all
nearly 200. The principal rivers are the Finn, which rises
near, the centre of the county and passes into Fermanagh,
and the Blackwater, which forms the boundary with Tyrone.
The Ulster Canal passes the towns of ^Ionaghan and
Clones, allbrding communication between Lough Neagh
and Lough Erne. Eskers occur at several places. There
are seams of unworkable coal in the south-west of the
county. The limestone is not only abundant and good,
but from the position of the rocks it can be obtained at
very small expense in working. Freestone and slates are
quarried in considerable quantities. The other minerals
include lead ore, antimony, fuller's earth, marble, and
maaganese; but the quantities obtained are inconsiderable.
CUmntc ami AgricuUnre. — Partly owing to the large proportion
of bog aud water the climate ia somewhat moist. The soil iu the
more level portions of the county is very fertile where it rests on
limestone, and there is also a mixed soil of deep clay, which is capa-
ble of high cultivation ; but in the hilly regions a strong retentive
tUy prevails, which could be made productive only by careful drain-
ing and culture. Spade husbandly generally prevails. Tlie most
common manure is a compost of lime and burned tutf mould.
Marl is abundant, but is little used, and gypsum also is found.
The number of holdings in 1881 was 17,849, of which as many as
10,784 did not e;:ceed 15 acres in extent, and 2870 of these did not
exceed 5 acres ; 6454 ranged between 15 and 50 acies, aud only 24
were above 200 acres. The area of arable laud was 278,755 acres, or
87 per cent, of the whole, while 6258 were under plantations, 'i^jSO
bog and marsh, 5239 barren mountain land, and 21,582 water, roads,
and fences. The following taVde shows'the aieas under the differ-
ent crops in 1850 and 1882 :—
1
5,661
1,228
1 |l
o 1 So
80,946 1 7,467
53,997 ; 1,665
i
s
s
&
22,105
21,321
1 li
7,190 2,543
7,50-.> , 1,533
^
s
E5
s
1850
1S82
10,157 ll.?«n
12,S48 1 31,450
147,683
131,134
Horses numbered 10,229 in 1872, and 10,666 in 1882. In the
same years mules numbered 300 and 469, and asses 4314 and 3476.
The number of cattle in 1872 was 81,333, and in 1882 only 72,266,
au average of 25 '9 to every 100 acres under cultivation, the
average for Ireland being 25-8. Sheep between 1872 and 1832
declined from 17,964 to U858, a very inconsiderable number; pigs
increased from 26,008 to 29,972 ; goats from 8873 to 12,391 ; aud
poulti-y from 341,874 to 434.260.
According to the latest return, the land was divided among 1470
proprietors, who possessed 311, 440acies, with a total annual value of
^261,382. The average size of the properties was 211 acres, and
the average value per statute acre 17 shillings. The following
seven proprietors possessed upwards of 10,000 acres: E. P.Shirley,
26,380 ; marquis of Bath, 22,762 ; carl of Dartrey, 17,345 ; Lord
Rossmore, 14,839 ; Sir John Leslie, 13,621 ; Viscount Templeto^vn,
12,845 ; A. A. Hope, 11,700.
Manu/aclurcs. — The only manufacture of consequence is nnen,
which of late years has been on the increase. The number of
scutching mills iu 18S1 was 55, of which 45 were WTOught by
water, 8 oy steatn, and 2 by water and steam.
Admi7iisiraiion. — The county includes 5 baionies, 23 parishes,
and 1850 town lands. Assizes are held at JFonaghan, and quarter-
sessions at Car rick macross, Castleblayney, Clones, and iMonaghan.
There are 8 petty sessional districts within the county, and part of
another. It includes the poor-law unions of Carrie kmacross and
Monaghan, and portions of Castleblayney, Clogher, Clones, Coote-
hill, and Dundalk. It is in the Belfast military district, sub-
district of Armagh. There is a barrack station at Monaghan. Id
the Irish parliament two members were returned for the county
and two for the town of llonaghan, but at the Union Monaghan
was disfranchised.
Fvpidaiiov.— The population in 1841 was 200,442; but in 1851
it had diminished to 141,823, in 1871 to 114,969, and in 1881 to
102,748, of whom 50,077 were males and 52,671 females. At the
last census 73 per cent, of the inhabitants were Rompn Catholics,
13 per cent. Episcopalians, and 11 percent. Presbyterians. The
number of emigrants from let May 1851 to Slst December 1881 was
56,408, or about 1840 persons per annum ; while during the twenty
-years ending 31st March 1881 the annual rate of emigration was
i3'8 per 1000 of the population. The death-rate to every thousand
of the population for the ten years ending 1881 was 16*9, the birth-
rate 23" ■), and the marriage-rate 3*6. The towns possessing more
than 1000 inhabitants are— Monaghan 3369, Clones 2216, Cariick-
macross 2002, Castleblayney 1610, and Ballyblay 1651. Monaghan.
the county town, received its name Muincchan (the town of monks)
from a monastery founded there at a very early period. The town was
incorporated by James I., but it was little more than a hamlet till
towards the close of last century. Besides the usual county buildings,
it contains a Roman Catholic college, and National model schools.
History and Antiqriitics. — In the time of Ptolemy, Monaghan
formed part of the territory of the Scoti. Subsequently included
in the district of Oriel or Orgial, and long known as i\Iacmahon*s
country, it "became shire ground in the reign of Elizabeth.
The antiquarian remains of Monaghan are comparatively unim-
portant. At Clones there is a round towcr.in good presen-ation,
but very rude in its masonry ; another at Inniskeen is very
dilapidated. Near Clones there are two large raths. Although
there are several old Danish forts, there are no niediiwal castles of
importance. The only monastic structure of which any vestiges
remain is the abbey of Clones, which was also the seat of a bishopric.
The abbey dates from the 6th century, but was rebuilt in the 14th
century after destruction by fu'o. On the site of the Franciscan
abbey at Monaghan a castle was erected, which was in a ruinous
condition in the time of James I.
MONARCHIANISM, in its teclinical Christoiogical
sense, designates the view_ taken by those Christians who,
M O K-
-within the church, towards the end of the 2d century
and during the 3d, opposed the doctrine of a hypostatic
Logos (hypostasianism) or of an independent personal sub-
sistence of the Divine Word. It is usual (and convenient)
to speak of two kinds of monarchianism, — the dynamistic
and the raodalistic. By monarchians of the former class
Christ was held to be a mere man, miraculously conceived
indeed, but constituted the Son of God simply by the in-
finitely high degree in which he had been filled with Divine
wisdom and power. This view was represented in Asia
Minor about the year 170 by the anti-Montanistic Alogi,
so called by Epiphanius on account of their rejection of the
Fourth Gospel ; it was also taught at Kome about the end
of the 2d century by Theodotus of Byzantium, a currier,
who was excommunicated by Bishop Victor, and at a later
date by Artemon, excommunicated by Zephyrinus. About
the year 260 it was again propounded within the church
by Paul of Samosata (q.v.), who held that, by his unique
excellency, the man Jesus gradually rose to the Divine
dignity, so as to be worthy of the name of God. Modalistic
monarchianism, conceiving that the whole fulness of the
Godhead dwelt in Christ, took exception to the " subordi-
natianism " of some church writers, and maintained that the
names Father and Son were only two different designations
of the same subject, the one God, who " with reference to
the relations in which He had previously stood to the world
is called the Father, but in reference to His appearance in
humanity is called the Son." It was first taUght, in the
interests of the "monarchia" of God, by Praxeas, a con-
fessor from Asia Minor.in Rome about 1 90, and was ojjposed
by TertiUlian in his well-known controversial tract. The
same view — the " patripassian " as it was also called, because
it implied that God the Father had suffered on the cross —
obtained fresh support in Kome about 215 from certain
disciples of Noetus of Smyrna, who received a modified
support from Bishop Callistus. It was on this account
that Hippolytus, the champion of hypostasian subordinatian-
ism, along with his adherents, withdrew from the obedience
of Callistus, and formed a separate community. A new and
conciliatory phase pf patripassianism was expounded at a
somewhat later date by Berj-llus of Bostra, who, while hold-
ing the di'nnity of Christ not to be ISla, or proper to Him-
self, but TrarpiK^ (belonging to the Father), yet recognized
iu His personality a new irpotnnrov or form of manifestation
on the part of God. Beryllus, however, was convinced of
the wrongness of this view by Origex (?.«.), and recanted
at the synod which had been called together in 2 44 to
discuss it. For the subsequent history of modaUstic mon-
archianism, see Sabellius.
MONASTICISM. See Monachism.
MONASTIK, BiToiiA, or Toli Monastir, a city of
Macedonia, now the chief town of the Turkish vilayet of
Roumelia, is situated at a height of 1880 feet above the
sea, in a western inlet of the beautiful, fertile, and many-
villaged plain which, with a breadth of about 10 miles,
stretches for 40 miles eastward from Mount Peristeri
(7714 feet high) to the Babuna chain. It is embosomed
in rich masses of foliage, and crossed by a rough-channeled
mountain stream, the Drahor, which joins the Czema or
Karasu, a tributary of the Vardar. The military advan-
tAges of its po.-<ition at the meeting-place of roads from
Salonica, Durazzo, Uskiub, and Adrianople led the Turks
dbout 1820 to make Monastir the headquarters of the
Roumelian corps cTarmee. Since then its general and
coTnmercial importance has greatly increased. A consider-
able amount of gold and silver work (especially clasps and
filigree) is made by the local craftsmen. The population
is about 40,000.
Monastir— so calleJ from the monastery of Bukova (The Beeches),
•omo himdred feet up the sloiie of Peristeri^^ia ideutifieJ with the
M O X
719
anci-nt Hericloa LjTiccstis on the Eimalian VToy ; and its biihopnc
is still caUcU ti'.e bishopric of ?cla,-oiiii from tlie aucicnt naiiii: of
the plain. In 1833 the town was the scene of the massarn. of the
Albanian heys.
MOXBODDO, James BtrKXETT. Lord (1714-1799),
author of works on the Oii>;in and Pnifirets of Lttnr/aaffe
(published in 1773), and Auciait JfetujI/ii/sics (1779), was
one of the most marked characters in Scottish literary
circles in the 18th century. He was born in 1714 at
Jlonboddo in Kincardineshire, studied at Aberdeen and
Groningen, and quickly took a leading position at the
Edinburgh bar, being made one of the Lords of Re.ssion
in 1767. Many of his eccentricities, both of conduct and
opinion, appear less eccentric to the present generation
than they did to his contemporaries; though he seems to
have heightened the impression of them by his humorous
sallies in their defence. He may have had other reasons
than the practice of the ancients for dining late and per-
forming his journeys on horseback instead of in a carriage.
His views about the origin of society and language and the
faculties by which man is distinguished from the brates
afforded endless matter for jest to the wags of his day;
but readers of this generation are more likely to be sur-
prised by the scientific character of his method and the
acuteness of his conclusions than amused by his eccentri-
city. These conclusions have many curious points of con-
tact with Darwinism and Neo-Kantism. His idea of
studying man as one of the animals, and of collecting facts
about savage tribes to throw light on the problems of
civilization, bring him into contact with the one, and his
intimate knowledge of Greek philosophy >vith the other.
In both respects Monboddo was far in advance of his
neighbours. His happy turn of Virgil's line —
"Xante molis erat humannm condere gentem " —
might be adopted as a motto by. the Evolutionists ; and
Neo-Kantians would find it hard to believe that he published
his criticism of Locke in 1773. His studied abstinence
from fine writing — from " the rhetorical and poetical style
fashionable among writers of the present day " — on such
subjects as he handled confirmed the idea of his con-
temporaries that he was only an eccentric concocter of
supremely absurd paradoxes. He died, 26th May 1799,
at the advanced age of eighty-five.
MONCTON, a town of the Dominion of Canada, in
Westmoreland, Kew Brunswick, 89 miles by rail north-
east of St John, is a port at the head of navigation on the
Petitcodiac, and the seat of the workshops and general
ofiices of the Intercolonial Railway. The popxilation,
about 1200 in 1871, was 5032 in 1881; the growth of
the place has been favoured by the establishment of sugar-
refining factories, and ftlctories for cotton and brass and iron
wares since the Canadian Parliament in 1879 adopted a
policy 01 protection. For the year 1881-82 the exports
amounted to $64,817, and the imports to 8252,571.
MON^DOXEDO, an ancient city of Spain, 27 miles
north-north-east from Lugo, in the province of that name,
is situated on the Sixto, a small tributary of the Masma,
on the Atlantic side of the Cantabrian chain, in a sheltered
site surrounded on all sides by considerable hills. The
population in 1S78 was 10,112. Thf,^incipal buildings
are the cathedral, a Corinthian structure of the 17th
century, an ex-convent of Franciscan friars of Alcantara,
which is now used for a theatre and a pablic school, and
the civU hospital. The industries, which are unimportant,
include lace-making, linen-weaving, and leather manu-
facture.
Accordine to local tradition, the bishopric of Dumitun, near
Braga, was transferred to San JIartin dc MondoSedo (three leagues
from llondohedo) in the 8th century ; it was brought to Mondo&edo
itself by Dofia Urraca in the beginning of the 12th century ; for
about sixty years prior to 1233.the see wasatBibadeo. After haviDg,
720
M O N — M O N
been for nearly a century and a half in the hands of the Moors,
MondoBedo was recaptured by OrdoBo I. in 858 ; and the Christian
possession waa made permanent by Alphonso III. in 870. It was
taken by surprise by the French in 1809.
MONDOVl, a city of Italy, in the province of Cuneo,
15 miles east of Cuneo and about 55 west of Genoa by
rail, was formerly the chief town of the Sardinian province
of Mondovi, and between 1560 and 1719 the seat of a
Pledmontese university. The central quarter occupies the
summit of a hill 1670 feet high, and contains the hexa-
gonal piazza, a citadel erected in 1573 by Emanuel PhiU-
bert, the cathedral of St Donatus, a spacious episcopal
palace, and the statue of Beccaria, who was a native of
the town. At the foot of the hill along the banks of the
EUero (a tributary of the Po) lie the industrial and
commercial suburbs of Breo, Borgatto, Pian della Valle,
and Carassone, with their potteries, tanneries, marble-
works, lie. The mansion of Count San Quintino in Pian
della Valle was the seat of the printing-press which from
1472 issued books with the imprint Mons Kegalis; and in
modern times the Ducal press founded by Emanuel Phili-
bert has acquired a great reputation. The population of
the town was 9637 in 1871, with the suburbs 11,958;
that of the commune 17,726 in 1861, and 17,902 in 1881.
Breo is identified with a qcrtaiu Colonia Bredolensis ; but Slon-
dovi proper — Mons Vici, Mons Kegalis (Monteregale), or Vicodunum
— probably did not take its rise till about 1000 A.D. The bishopric
dates from 1388.
MONEY
1. Definition and Functions of Monet/. — The precise
definition of Money is a question presenting no small
difEcvUty, and it has been complicated by the attempts of
some writers to define the term so as to lend support to
their favourite theories. The real difficulties of the subject
are, however, chiefly connected with paper-money, and as
that side of the question has been dealt with in the article
Banking (?.».) it will here be sufficient to adopt the clear
and careful da^cription of money given by a distinguished
American economist as being " that which passes freely
from hand to hand throughout the community in final dis-
charge of debts and full payment for commodities, being
accepted equally without reference to the character or credit
of the person who offers it and without the intention of the
person who receives it to consume it or enjoy it or apply it
to any other use than in turn to tender it to others in dis-
charge of debts or payment for commodities." ' In this
passage the essential features of money are plainly set forth,
though, as is frequently the case in economics, particular
cases hard to bring within the description may be found. ^
The functions which money discharges in the social
organism are — at least in the opinion of all writers worth
noticing here — clearly manifest. The most important is
that of facilitating exchanges. It is not necessary to dwell
on the great importance of this ofiice. The mere consider-
ation of industrial organization shows that it is based on
the division of employments ; but tlie earliest economic
writers saw clearly that division of employments was
rendered possible only by the use of a medium of exchange.
They saw that the result of increasing specialization of
labour was to bring about a state of things in which each
individual produced little or nothing directly adapted to
satisfy his ewn wants, and that each one was to live by
exchanging his products for those of others. They saw,
moreover, that this was not feasible \vithout some object
which all would be willing to accept for their peculiar pro-
ducts, for otherwise, the difficulty of getting those together
whose wants were reciprocal would be a complete hindrance
to the develojiment of exchange, which alone made division
of labour possible. A second function hardly inferior in
importance to the one just mentioned is that of affording
a ready means of estimating the comparative value of dif-
ferent commodities. Without som.e common commodity as
a standard of comparison this would be almost impossible.
" If a tailor had only coats and wanted to buy bread or a
horse, it would be very troublesome to ascertain how much
bread he ought to obtain for a coat or liow many coats he
' F. A. Walker, Mmey, Trade, and IndHstry, p. i.
- For further information as to the discussions relative to the proper
definition of " Money," the reader may consult J. S. Mill, Prin. of Pol.
Eton., B. iii. ch. 12, § 7 ; Jcvous, Honey, pp. 248 sq.; i,. do
Lnveleye, Marchi Monllaire, pp. 226 sq.; ami especially Mr H.
Sidgwick's article " What is Money ! " in the Foriniijhtly Review
(April 1879), also his PritKiples of Political Economy, pp. 231 .17.
should give for a horse ; " ' and as the number of com-
modities to be dealt with increased the problem- would be-
come harder, " for each commodity would have to be quoted
in terms of every other commodity." Indeed it may be
reasonably maintained that the idea of general value could
not be formed without the existence of money, and all that
is known of savage races tends to bear out this view.* The
adoption of some one commodity renders the comparison
of values easy. "The chosen commodity becomes a common
denominator or common measure of value in terms of which
we estimate tho values of all other goods," ^ and thus money,
which in its primary function renders exchanges possible by
acting as an intermediate term in each exchange, also makes
exchanges easier by making them definite. Another func-
tion of money comes into being with the progress of society.
One of the most distinctive features of advaiicing civiliza-
tion is the increasing tendency of people to trust each
other. Thus there is a continual increase in relations of
contract, as may be seen by examining the development of
any legal system. Now a contract implies something tO'
be done in the future, and for estimating the value of that
future act a standard is required ; and here money, which
already acts as a medinm of exchange and as a measure ofvalui
at a given time, performs a third function, by affording an
approximate means of estimating the present value of the
future act, and in this respect may be regarded as a standard'
of value, or, if the phrase be preferred, of deferred payments.^
Some writers attribute a fourth function to money, inas-
much as they regard it as being a means of easily storing
up value. Doubtless it does supplj- this need, which is a
specially pressing one in early civilizations owing to the
insecuritj' vfhich then exists, but with the progress of
settled government the need becomes less extreme. Other
forms of investment grow up, and the habit of hoarding
money becomes unusual. It is therefore better to regard
the functions of money as being only three in number, ^'iz.,
to furnish — (1) the common medium by which exchanges
are rendered possible, (2) the common measure by which
the comparative values of those exchanges are estimated,
and (3) the standard by which future obligations are
determined.
2. C auscs which Determine the Value of itoney. Quantity
of Money needed by a Nation. — The problem of the deter-
mining causes of the value of money is a particular case of
the general problem of values, but there are circumstances
which render the inquiry more than usually complicated.
Before considering these it will be well to deal with a use
of the phrase "value of money" which has led to much con-
' Mill, Prin., B. iii. ch, 7, § 1.
■• W. Bagehot, Economic Studics,fxi. 42-J3. = Jevons, Money, p. 6.
* For an ingenious argument ngniust the use of the terms " measure '
and "standard" of value, see F. A. Walker, Money, pp. 4 sq., 12, and
Money, Trade, and Indnstry, pp. 27 517., CO sq. Tlie shorter title i:
uniformly used here for his larger treatise.
MONEY
721
<famon. ' In mercantOe phraseology the Talue of money
means the interest charged for the vise of loanable capital
Thus, when the market rate of interest is high money is
said to be dear, when it is low money is regarded as cheap.
Whatever may be the force of the reasons in favour of this
ose, it is only mentioned here for the purpose of excluding
it. For our present subject, " the value of a thing is what
it will exchange for ; the value of money is what money
will exchange for, or its purchasing power. If prices are
low, money will buy much of other things, and is of high
value ; if prices are high, it vcill buy little of other things,
and is of low value. The value of money is inversely as
general prices, falling as they rise and rising as they fall." >
Now in the general theory of value it appears that the
proximate condition which determines it is the equation
between supply and demand; and this is clearly the case
with reference to money. These terms, supply and demand,
need, however, some elucidation. Let us consider what is
meant by the supply of, and demand for, money. The
supply of a commodity means the quantity of it which is
offered for sale. But in what shape does the sale of money
take place t By being offered for goods. " The supply of
money, then, is the quantity of it which people are wanting
to lay out;" or, to put the point more concisely, it is "all
the money in circulfition at the time." Again, to take the
case of demand, — the demand for a commodity is the pui--
chasing power offered for it.- Demand in the special case
of money consists of all the goods offered for sale. There
is, however, a peculiar featiu*e in the case of money which
arises from its position as the medium of exchange, viz.,
that money is, so to say, in a " constant state of supply
and demand," since its principal service is to act as the
means of purchasing commodities.' From this it follows
that the factors which determine the value of money within
a given time are : (1) the amount of money in ciroidation,
and (2) the amount of goods to be sold. On closer exami-
nation it will, however, appear that there are other elements
to be taken into account. In the first place, the quantity
of money is not by itself the sole element on the supply
side. In some instances a coin, will not circulate more
than two or three times in a year, while another coin may
make hundreds of purchases. In determining the value of
money these varying rates of circulation have to be con-
sidered, and by taking an average we may estabUsh the
existence of a fresh element to be estimated, namely, the
average rapidity with which money does its work, or, to
use Mill's expression, "the e£Bciency of money." On
the side of demand, again, it is not the quantity of commo-
dities that is the determining element, but the amount of
sales, and the same article may, and generally does, pass
through several hands before it reaches the consumer.
From this it follows that (if the consideration of credit in
its various forms be omitted) the value of money is inversely
as its quantity multiplied by its efficiency, the amount
of transactions being assumed to be constant. This formula
requires, however, some further explanations before it can
be accepted as a full expression of the truth on the subject.
It must be noticed that it is not commodities only that are
exchanged for money. Services of all kinds constitute a
large portion of the demand, while the payment of interest
on the various' forms of obligation requires a large amount
■)f the circulating medium. The potent influence of credit
Jso must be dwelt on. This latter force is the main element
to be considered in dealing mth variations of prides ; but
« Mill, Prin., B. iiL ch. 8, § 1.
= For a cleir statement of this, Eee J. R Caimes, Leading Principle!:,
part i. ch. 2.
' The leadins exception to this is in the case of money \:\.\cu is
loarded for an iude&nite period, and is therefore withdrawn fiom cir-
^olatioo.
10— 2G
BO far ELS it is based on a deposit of metallic money it may
be looked on as a means of increasing the efficiency of
money, and therefore as coming within the formula given
above. In its other aspects it lies outside the range of
this article. Some interesting conclusions may be deduced
from the resnits we have arrived at. One of these is that
the " increased development of trade," or "expansion of
commerce," of itself tends to lower not to raise prices;
for, by increasing the work which money has to do while
th« amount remains the same, it raises its value.* Another
Consequence is that a large addition may be made to the
money in a coimtry without any effect being produced on
prices. This is evident, since money only acts on prices
by being brought into circulation ; therefore, if the money
which is added to the national stock is not used in this
way, prices will remain unaffected.
We have now sufficiently considered the proximate con-
ditions which determine the value of money ;_ the next step
is to inquire : What is the ultimate regulator of its value ?
The value of freely-produced commodities is — according to
the ordinary theory of economists- — determined by their
" cost of production," or, where the article is produced at
different costs, by the cost of production of the most costly
portion. We have now to consider how far this theory
applies to the special case of money. Gold and silver, the
principal materials of money, are the products of mines,
and are produced at different costs ; therefore the cost of
the part produced at greatest cost ought to determine their
value. This theory is, however, true only under certain
conditions^ — namely, that competition is perfectly free, and
that there are accurate data for computing the cost of pro-
duction, and even then it is true only " in the long run."
Moreover, cost only operates on value by affecting supply.
" The latent influence," says Mill,* " by which the values
of things are made to conform in the long run to the cost
of production is the variation that would otherwise take
place in the supply of the commodity." From these con-
siderations it follows that cost of production does not so
influentially affect the value of money as some writers have
supposed. In former periods it was a common proceeding
on the part of the state to either restrict or stimulate coin-
age and mining for the precious metals. At all times the
working of gold and silver mines has been rather a hazard-
ous speculation than a legitimate business. " When any
person undertakes to work a new mine in Peru," says Adam;
Smith," " he is universally looked upon as a man destined
to bankruptcy and ruin, and is upon that account shunned
and avoided by everybody. Mining, it seems, is considered
there in the same light as here, as a lottery, in which
the prizes do not compensate the blanks ; " and all subse-
quent experience confirms this view. With regard to the
adjustment of supply to meet an altered cost of production,
the difficulties are, if possible, still greater. The supply
of money is so large compared with the annual production,
that any change can operate but slowly on its value. The
total stoppage of fresh supplies firom the mines would not
be felt for some years in the increased value ; and an in-
creased amount of production, though more rapid in its
operation, takes some time to produce an effect. " Hence
the effects of all changes in the conditions of production of
the precious metals are at first, and continue to be for many
years, questions of quantity only, with Uttle reference to
cost of production." On these grounds it is apparent that
cost of production is not, for short periods, the controlling
force which governs the value of money, and even for long
* This view, which seems to most persons a p.iradox, is well put by
Adam Smith, Wealth of Kations, p. 81 (ed. M'Culloch) ; also by J.
E. Caimes, Essays mi Political Ecommy, p. 4.
« Prin., B. iii. ch. 3, § 2.
» Wealth o/A'atims, p. 78 (cd. M'Culloch).
722
MONEY
periorls the speculrttivo naturo of ttia industries connected
■with the production of money renders the cmi of produc-
tion an element very hard to ascertain. Another considera-
tion which gives a peculiar feature to the problem of money-
value is that in the ca^e of other commodities a change in
cost of production affects value without any actual change
in the supply. The knowledge that a commodity can be
produced at a lower cost will cause a reduction in its value.
This is not true of money. Either the quantity or the
efficiency of money must be altered to change its value.
This is, of course, a result of its position as the circulating
medium. When all these circumstances are taken into
account it becomes clear that the most correct way to
regard the question of money-value is that which looks on
supply and demand, as interpreted above, as the regu-
lator of its value for a limited time, while regarding cost
of production as a force exercising an influence of uncer-
tain amount on its fluctuations during long periods. Where
the coinage of a state is artificially limited, the value of
its money plainly depends on supplv and demand as we
iave interpreted it.
The next question which arises is ; What quantity of
■money does a nation require ? What amount of the circu-
lating medium is necessary for the proper working of the
industrial organism 1 To this puzzling problem the earlier
economists gave answers in the shape of definite formulas.
Thus, Sir W. Petty was of opinion that the amount of coin
required by a country was one-half the rent of land, one-
fourth the amount of building rent, and one fifty-second
part of the annual wages of labour. Locke's view was- that
one-fiftieth of labourera' wages, one-fourth landowners'
revenue, and one-twentieth of traders' yearly returns, was •
the proper amount. Modern statisticians, however, though
having command of much greater resources, decline to
attempt a quantitative answer, and content themselves
■with indicating the conditions which the problem involves,
in fact we must first examine the work which money has
to perform, and this depends on several conditions. The
first of these is the population ; cseteris paribus, twice as
many people ■will want twice as much money. The second
is the amount of transactions ; for, if the amount of busi-
ness done is doubl d, the amount of money must be also
doubled, unless at the same time some improvement in credit
is introduced. The efficiency of money b a third element
■which aflfects the quantity needed, and this is largely
dependent on the habits of the people and the facilities for
communication. Other elements which can be ordy briefly
indicated are — -" the degree in which credit exists between
man and man ; the amount of travelling which takes place ;
and the commercial and banking organization which exists." '
Another factor which reqidres to be estimated is the extent
to which habits of hoarding exist ; for all money hoarded
is withdrawn from circulation, and therefore increases the
total amount needed. The habits of saving in the rural
dbtricts of France remarkably exemplify this element in
the question. Again, the existence of barter does away
■with the use of so much money as would be required to
carry on the exchanges effected by barter. The custom
of paying wages in kind has a similar effect. This bare
statement shows how insoluble the question is. 'Wlien we
contemplate the matter from an international point of
view, the amount needed, after allowance is made for the
cost of transporting goods, is plainly that which will keep
a country's prices at a level with those of the countries
•with which it has commercial relations.^ For otherwise
the country woidd have an excess either of importation or
of exportation, which would necessitate a flow of money to
the country whose prices were lov/er than the general level.
I F. A. Walker, Honey, p. 73.
li., p. bl.
This, then, Is the condition wWch determines couijiarative
prices between different countries ; and, prices being so
determined, the quantity of money needed to keep up those
prices depends on the conditions above indicated. In tho
case of England reliable statistics t«nd to show that the
gold in circulation wa.s, in 1872, about £105,000,000, and
the note circulation £13,000,000. In any Continental
country the amount would probably be proportionally much
greater, owing to the fact that there is in England a greater
development of credit.
3. Early Fonm of Currenry. — Up to the present we have
considered money <is being fully established and properly
adapted to fulfil its various functions. We have now to
trace the steps by which a suitable system of currency was
evolved from a state of barter. It is important for a right
understanding of the question to grasp tho ft.ct that ex-
changes took i>lace originally between groups, and not
between individuals. This explains the slow growth of
exchanges, as each group produced most of the articles
necessary for itself, and such acts of barter as took place
were rather reciprocal presents than mercantile exchanges.
Such is actually the case at present among modem savages.
" It is instructive to see trade in its lowest form among
such tribes as the Australians. The tough greeristone
valuable for making hatchets is carried hundreds of miles
by natives, who receive from other tribes in return the
prized products of their districts, such as red ochre to paint
their bodies with ; they have even got so far as to let
peaceful traders pass unharmed through tribes at war, so
that trains of youths might be met, each lad with a slab of
sandstone on his head to be carried to his distant home
and shaped into a seed-crusher. ^Maen strangers ■visit a
tribe they are received at a friendly gathering or cor-
robboree, and presents are given on both sides. No doubt
there is a general sense that the gifts are to be fair
exchanges, and if either side is not satisfied there ■will be
grumbling and quarrelling ; but in this roughest kind of
barter we do not yet find that clear notion of a unit of
value which is the great step in trading."^ This vivid
description of what is going on at present among lower
races enables us to realize the way in which money came
into existence. WTien any commodity becomes an object
of desire, not merely from its use to the persons desiring it,
but from their wanting it as being readily exchangeable
for other things, then that article may be regarded as rudi-
mentary money. Thus the greenstone and ochre are on
their way to being promoted to the position of currency,
and the idea of a " unit of value " is all that is needed to
complete the invention. " This higher stage is found among
the Indians of British Columbia, whose strings of haiqua-
shells worn as ornamental borders to their dresses serve
them also as currency to trade with,- — a string of ordinary
quality being reckoned as worth one beaver's skin." * These
shells, therefore, are in reality money, inasmuch as thev
discharge its functions.
On a review of existing savage tribes and ancient races of more
or less cinlirjitiou we are surpiised at the creat variety of obje'-ts
which hare been used to supply the need of a circulating medium.
Skins, for instance, seem to be one of the earliest fonns of money.
They are to be found at present amonf; the Indians of Alaska' dis-
charging this service, while accounts of leather money seem to show
that their use was formerly more general. As the hunting sta"o
gives place to tlio. pastoral, and animals become domesticated, the
animal itself, instead of its skin, becomes the principal form of cur-
rency. There is a great mass of evidence to show that, in the most
distant regions and at very different times, cattle formed a currency
for pastoral and early agricultural nations. Alike among existing
barbarous tribes and in tho survivals discovered among classical
nations, shern ard oxen both appear as units of value. Thus w«
lind that at Kc-nc, and through tho Italian tribes generally, "oxen
and sheep farmed tho oldest medium of exchange, ten sheep beinjj
' E, B. Tylor, Antlircpotojrj, pp. 281-282.
' Tylor, loc. cit. ' Whympor, Alaska, p. 286.
MONEY
723
fad:oned equivalent to one ox. The recognition of these objects as
t^urersal legal representatives of value, or, in other words, as money,
may be traced back to the epoch of a purely pastoral erouomy. "*
The Icelandic law bears witness to a similar state of thiags ; while
the viriovn f:p.es in the different Teutonic codes are estimated in
cattlj. 'It., Larin word jwctmio (pjcu5) i.i an evidence of the earliest
"Roman mouey being composed of cattle. The English fee and the
famous term /eitdal, according to its most probable etymology, are
derived from the same root In a well-known passage of the Iliad'
the value of two different seta of armour is estimated in terms of
oxen. The Irish law tracts bear evidence as to the use of cattle as
one of the measures of value in early Irish civilization.' Within
the last few years it has been prominently brojght before the public
that oxen form the principal wealth and the circulating medium
smong the Zulus and Kaffrea. On the testimony of an eye-witness
ve are assured that, "as cattle constitute the sole wealth of the
people, so they are their only medium of such transactions as involve
exchange, payment, or reward."* We find that cattle-rents are
TOid by the pastoral Indian tribes to the United States Government'
From the prominence of slavery in early societies it is natural to
suppose that slaves would be adopted as a medium of exchange, and
one of the measures of value in tne Irish law tracts, eumAal, is said
to have originally meant a female slave. They are at present applied
to this purpose in Central Africa, and also in New Guinea. On
passing to the agricultural stage a greater number of objects are
found capable of being applied to currency purposes. Among these
are corp — used even at present in Norway— maize, olive oil, cocoa-
nntSj and tea. The most remarkable instance of an agricultural
product being used as currency is to be found in the case of tobacco,
which was adopted as legal tender by the English colonists in North
America. Another class of articles used for money consists of
ornaments, which among all uncivilized tribes serve this purpose.
The haiqua-shells mentioned before are an instance, cowries in
India, whales' teeth among the Fijians, red feathers among some
South Sea Island tribes, and finally, any attractive kinds of stone
which can be easily worked. Mineral products, so far as they do
not come under the preceding head, furnish another class. Thus
salt was used in Abyssinia and Mexico, while the metals — a pheno-
menon which will require a more careful examination — have suc-
ceeded in finally driving all their inferior competitors out of the
field, and have become the sole substances for money at present.
4. Metallic Forms of Money. Their Superiwity over
other Subatancea. Special Admntages of Silver and Gold. —
The use of metals as a form of money can be traced far back
ia the history of civilization, but, as it is not possible to
ascertain the historical order of their respective adoptions
for this purpose, we will take them in the order of their
•value, beginning with the lowest. Iron, judging from the
statement of Aristotle, was extensively employed as currency.
One remarkable icstance of this which at once occurs to the
mind is the Spartan moiiey, which is clearly a survival of
the older system that had died out among the other Greeks,
though by modem writers it has been attributed to ascetic
policy. In conjunction with copper, iron formed an early
Chinese currency, and till recently it was a subsidiary
coinage in Japan. Iron spikes are used in Central Africa,
while Adam Smith notices the use of nails for money in
Scotland.' Lead has also served as money, as it does at
present in Burmah. Copper has been more widely employed
than either of the previously-mentioned metals. Its use in
■|China as a parallel standard with iron has just been men-
tioned. The early Hebrew coins were chiefly composed of
it, while do«-n to 269 b.c. the sole Roman coinage was
-an alloy of copper. Till a very recent period it formed the
principal moneyof some poorer European states (as Sweden),
■and V. as the subsidiary coinage of the United Kingdom till
the present bronze fractional currency was introduced. Tin
was not so favourite a material for money as copper, but
the early English coinages were composed of it, probably on
account of the fertile tin mines of Cornwall, and in later
times halfpence and farthings of tin hn\ e been struck. The
' Jloramsen. fflsl. of P.omt {Eng. trans.), i. p. 203.
' The episode between Diomede and Glaucus in the 6th book.
" Maine, Early Historij of Instiliilions, Lect. vi. ; Brihon i^aw
Tincti (ed. by Drs Haiicoik and Richey).
* P.ev. H. Diigmore, quoted by Maine, op. n't., p. 143
• F. A Walker, Money, Trade, and Indualry, p. 22.
« n'laltli of Vadoiu, p. 11.
i."exv metal which comes into notice is silver, which up to
the last few years was the principal form of money, and
even still is able to dispute the field with its most formidable
livaL It formed the main basis of Greek coins, and was
introduced at Rome in 269 B.C. The mediaeval nloney was
principally composed of silver, and its position 'Ji recent
times will have to be subsequently noticed more at length.
Gold which is the most valuable of the metals widely used
for monetary purposes, has been steadily gaining ground
with the growth of commerce. The earliest trace of its use
in common with that of silver is to be found " in the pictures
of the ancient Egyptians weighing in scales heaps of rings
of gold and silver." ' The only other metals used for money
— platinum and nickel — may be easily disposed of. The
former of these was coined for a short time by the Russian
Government, and then given up as unsuitable. The latter
is only used as an alloy.
The examination of the forms of currency, both metallic
and non-metallic, in which we have been engaged leads to
certain definite conclusions as to the course which the
evolution of currency is pursuing. It appears (1) that the
metals tend to .supersede all other forms of money among
progressive peoples, and (2) that certain metals tend to
supersede the others. From this we are led to consider the
qualities which are desirable in the material of money, and
to conclude that the presence or absence of those qualities
is the reason of the adoption or rejection of any given
substance.
(1) In the first place, it is neicessary that the material of
money should be desirable, or, in other words, possess value ;
and to this condition all the commodities we have reviewed
conform, for otherwise they would never have attained the
position of being a medium of exchange. This quality,
then, is not the reason for the preference of some forms over
others. (2) The second requisite clearly is that the value
of the article shall be high in proportion to its weight or
bulk, or, to put the same truth in another way, it is requisite
that it shall be portable. Want of this quality has been a
fatal obstacle to many early forms of money retaining their
place. Skins, com, and tobacco were found very difficult
to transfer from place to place. Iron and copper too
suffered from the same defect, while sheep and oxen, though
moving themselves, were expensive to transfer. (3) It is
further desirable that the material of money shall be the
same throughout, and that one imit shall be equal in value
to another. This is a reason for rejecting the widespread
currency composed of cattle, as the difference between one
and another head is of course often considerable. The
metals possess a particular advantage in this respect, as,
after being refined, they are almost exactly homogeneous.
(4) A fourth requisite is that the substance used as money
can without damage be divided and, if needed, united again;
here also the detired quality is peculiarly possessed by the
metals, as they are easily fusible, while skins or preciotia
stones suffer greatly in value by division, and it need hardly
be added that the same is the c?se with regard to animals.
(5) Money must also be durable. This at once removes
from the articles suitable for money all animal and many
vegetable substances. Eggs or oil will not keep, and conse-
quently soon lose their value. Iron, too, is liable to rust,
which, combined with its low value, is a reason for its dis-
us<^as currency. (6) Money should be easilydistinguishable,
and there should be no trouble in ascertaining its value.
This condition is one of the reasons why precious stones
have never been much used as money, their value being hard
to estimate. The same objection applies to most non-
metallic currencies, and is only obviated even in their case
by the process of assaying. (7) The last condition whicl
' Tjlor, p. 283
724
M O J< E Y
appears desirable for the money material is, that its value
shall be steady. This, however, is of but slight impo'-tance
in early societies, and it is only as deferred payments become
a prominent feature of industrial life that this requisite is
much needed. It is enough for the other purposes of money
that it shall not va'r<>- within short periods, which is found
to ba a feature of metals, and especially of silver and gold,
while corn especially varies mdely in value from season to
season. From the foregoing examination of the requisites
desirable in the material of money it is easy to deduce the
"empirical laws which the history of money discloses, since
metals, as compared with non-metallic substances, evidently
possess those requisites in a great degree. They axe all
durable, homogeneous, divisible, and recognizable, and in
virtue of these superior advantages they are the only
substances now used for money by advanced nations. Nor
is the case different when the decision has to be made
between the different metals. Iron has been rejected
because of its low value and its liability to rust, lead from
its extreme softness, and tin from its tendency to break.
Both these roetab, as well as copper also, are unsuitable
from their low value, which hinders their speedy transmission
so as to adjust inequalities of local prices.
The elimination of these metals leaves silver and gold as
theonlysuitablemateriaisfor forming Ihe principal currency.
Of late years there has been a movement towards the
ado^jtioD of the latter as the sole monetary standard, silver
being regarded as suitable only for a subsidiary coinage.
Indeed this question, which is reserved for subsequent
discussioUj may be regarded as the principal matter of
controversy in the field of metallic currency. The special
features of gold and silver which render them the most
suitable materials for currency may here be noted. " The
value of these metals changes only by slow degrees ; they
are readily divisible into any number of parts which may
b9 reunited by means of fusion without loss ; they do
not deteriorate by being kept ; their firm and compact
texture makes them difficult to wear ; their cost of pro-
duction, especially of gold, is so considerable that they
pDssess great value in small bulk, and can of course be
transported with comparative facility^ and their identity
is perfect." * The possession by both these metals of all
the qualities needed in money is more briefly but forcibly
put by CantiUon when he says that " gold and silver alone
are of small volume, of equal goodness, easy of transport,
divisible without loss, easily guarded, beautiful and brUliant,
and durable almost to eternity."^ This view has even been
pushed to an extreme form in the proposition of Turgot,
that they became universal money by the nature and force
of things, independently of all convention and law, from
which the deduction has been drawn that to proscribe silver
by law is a violation of the nature of things.^
5. Coinage: its Advantages, and ihe Pnncipal Questions
connected therewith. — The development of monetary systems
has now been traced down to the establishment of metallic
(.urrencies. These, in the early stages of their existence,
passed by weight. The Hebrew records jbear witness to
this fact, as also do the Greek writers. A^iatotle, fop ex-
ample, after indicating the circumstances which led to the
mvention of currency, proceeds to point out that it was
"afterwards determined in value by men putting a stamp
upon it, in order that it mo-y save them from the trouble
of weighing it." * There are two distinct stages in the
' Enq/. Brit. (8tb od.), art. "Money," vol. xv. p. 417.
■ W. S. Jevona in the Contemporary Revieto, January 1881. See also
Lord Liverpool, Coins of the Jtealm, (Bank of England reprint), p. 10.
1 Caimes, Logical ^fcthod of Pol, Econ., p. 131, note; and for
FoH.'nev., July 1831,
application of the argument to Bimt'tallisi
do Laveleye,
Pet, i. 9, S. The whole passage is wou'uy of quotation, as
Bhowing how clearly AristoUo conceived the primary fuoctlou of
introduction of coining. In the first, only tne quality or
fineness of the metal is denoted by the stamp, no attempt
being made to fix the weight. Ill other words, the stamp
acts as a kind of hall-mark. The Chinese cubes of gold
may have been the earliest money. Herodotus attributes
the first use of coined gold and silver to the Lydians,' while
in another passage he mentions that the first Greek coinage
was at iEgina, by Pheidoil of Argos.^ The second step
was to certify the weight as well as the fineness of the
metal, thus completing the invention. The necessity of
preventing any interference with the coin after it had been
stamped led to the adoption of a regular form, and, though
hexagonal or octagonal coins are to be found, the received
shape of a coin is that of a fiat circle, each side of which ia
stamped, as well as in many cases the edge. By this con-
trivance all persons into whose hands the coin came had a
guarantee as to its quahty and quantity, and we may reason-
ably infer that the great improvement in coinage among
the Grecian colonies was the eff'ect, and also in some degree
the cause, of the expansion of their commerce iji the 6th
century B.C. From Greece the art of coining spread to
Italy, being introduced by the Greek colonists in Lower
Italy. Since then coinage as an art has always existed in
the more advanced societies. The progress of invention,
however, does not end with the introduction of the art of
coining, since a number of practical questions arise with
reference to the best system to be adopted, which for a
protracted period present great difficulties to those who are
called upon to solve them. One of these, before touched
on, is ; What is the best shape for coins ! The answer has
finally been in favour of the circular, but square and oblong
pieces are also to be found.'' Closely allied with this is
the question of the most suitably Ikajts of size. The in-
ferior limit is plainly fixed by the convenience of those
using the coins. They ought not to be so small " that
they can be easily lost, or can with difficulty be picked
up." ' Instances of violations of this principle occur in the
case of the English threepenny piece and the American
one-dollar gold piece. The superior limit is a more difficult
point. Its determination turns partly on the difficulty of
coining large pieces, and partly on the facilities which such
large coins as the American gold double-eagle give for im-
proper treatment.- It\is an easy process to driU holes,
which can be concealed by hammering, VhUe in some cases
the coin has been sawn -in two, and the interior gold
removed, the outside surfaces being soldered together, while
platinum ia put in the midst to maintain the weight. As
a general rale it may be laid down that no gold coin much
larger than the English sovereign, or silver one at all larger
than the half-crown, should be issued. Another considera-
tion to be borne in mind when determining the proper
size of coins is the relative amount of wear which takes
place. Experience proves that large coins are less worn
than small ones. " According to experiments made at the
mint in 1833, the loss per cent, per annum on half-crowns
is about 2s. 6d., on shillings, 4s., and on sixpences, 7s. fid."
This result has been confirmed by other inquiries. From
this it follows that the larger coins are less expensive, but
their size is hmited by the fear of their being tampered ^
with. Again, the character of the stamp to be impressed
iiioDcy : 5l6 irpb% rds dX\a7d5 Toiovrtiv ri cvvtdevro jrpAj atpai
avToin SiSiviu «al 'Ka/iPireii', S t^p xwtf'/'wi' auri ip f^x^ T-j)*
X/Jcfaf tv/ieraxfipt'^rov Trpi)i t6 l^i)f, ohv ffi5i]poi kclI ipyvpos, k&p tt Tt
Toioi>roi' Irtpov, t4 liif rpCiroy dirXii ipicrOip liCfiOfi Kal trraS/i^, ^i
5* reXfVTaiop Kal xapaicTTipcL ijrifiaWiirruv, Xna iwoMaji Trjt /itTp^tm
* Herodotus, i. 94.
' lb. vi. 127. See also for a discussion of Pheidon's coinage,
Grote, kist. of Grace, ii. pp. 319 .-}. (Cabinet ed.).
' An instance of the latter is the ilxilm of the Japanese coinage,
•which is an oblong flat piece of eilv<-r.
' Jcvons, Money, p. 155.
MONEY
725
u a' matter requiring much care. The. objects aimed at
• in imposing the stamp are (1) to prevent the coin being
counterfeited, and (2) to prevent any of the metal being
abstracted. The former of these objects can be best at-
tained by making the device such as co.n be obtcincd only
by pow'erful and expensi%'0 mat:i'.ncry. The most improved
methods must be adopted, and the greatest pains taken to-
have the device perfectly executed. The latest improve-
ment in the process of coining is the introduction of the
knee-joint press. The latter difficulty is best obviated by
Tising special care in marking the edges of the coins. Ancient
coins were issued with unstamped edges which presented
no impediment to clipping, but modem coins, at least those
of any size, are protected by the edge being milled or by a
legend being inscribed round it. The combination of milled
«dges with a raised legend would be a still more effectual
means of protecting the coinage from interference.
Another matter of importance in the process of coining
is the nature and proportion of alloy to be used. The
necessity for some mixture arises from the fact that gold
and silver are both naturaUy soft, and, to obviate this, cop-
per has been mixed with them, so as to. produce a harder
substance. The Austrian ducat is the nearest approach to
purity among the principal coins of Europe, being com-
posed of seventy-one parts of pure gold to one of alloy.
The English gold coins are eleven-twelfths pure gold, while
the silver ones are thirty-seven-fortieths pure silver. The
origin of the difference is purely historical The general
gold proportion is nine-tenths gold to one-tenth alloy, while
in some coinages the proportion of silver to alloy lb nearly
five to one, the countries composing the Latin Union
having adopted that proportion in order to reduce their
smaller silver coins to tokens. Copper is the usual material
for alloying, but the Melbourne mint used silver for some
time. It is this silvery alloy that accounts for the yellow
appearance of many Australian sovereigns. They, however,
are rapidly disappearing, as it is profitable to melt them
down. It has been mentioned above that the wear of
small coins ia greater than that of large ones, and it
may be added here that the wear of coins in general is an
important question in connexion with their legal circula-
tion. The English sovereign is believed to remain above
the least current weight for from fifteen to twenty years.
For the technical processes of coining, (tc, reference may be
^ade to the article Mint.
The next topic to be considered is : Who should issue
money? In the earlier stages of currency the question
was not so prominent, but the establishment of coining
brought it forward. In Greece each city being autono-
mous claimed, and exercised the right of freely coining as it
desired, the coins being, of course, received in other cjties
only at their real value. The consequences of this system
were generally beneficial. The Greek coins were usually
up to their nominal value, as debased coinage was imable
to circulate beyond the place of issue, and therefore ex-
tremely inconvenient to the members of the state issuing
it.' Under the Roman republic private persons were
probably allowed to bring metal to be coined, though the
coins seem generally to have had the name of one of the
consuls for the year on them. Under the empire the
doctrine became established that the right of coining be-
longed exclusively to the emperor, and till the fall of the
\Vestern empire this was acted on. After the establish-
ment of the various barbarian kingdoms, each sovereign
assumed the privilege pf coining, a right which in France
was extended. to or rather usurped by the principal nobles.^
In England th^ king alone coined silver.^ At present the
1- See Lenormant, Contemp. Jiev., February 1879.
■ Hallam, Middle Ages, L pp. 205-206.
• Lord Liverpool, Coint of the Seaim, ch. t.
control of the operations of the mint is completely in the
hands of the executive ; and, until recently, no question on
theoretical grounds as to the propriety of this method haa
ever been raised.*
In clo;3 connexion ■with the right of coining comes
the consideration as to the proper persons to bear the
expense of tije process. At first sight the answer seems
plain enough. Coins are a manufactured article quite
as much as plate, and are rendered more valuable by
being assayed, weighed, and certified. It appears there-
fpre quite proper that those who bring metal to be
coined should bear the expense of the coinage, or, in
other words, should give up a part of the metal to the
mint, thus paying for the service rendered to them in the
same manner as those sending letters pay the postal de-
partment for their transmission. This course has been
usually adopted. England, however, has taken a different
line. In order to encourage the coining of the precious
metals, no charge was made at the mint beyond that in-
volved in the necessary delay in the operation ; aitd this is
at present the case with gold. Though this arrangement
was originally introduced in obedience to the prejudices of
the mercantile system which regarded gold and silver as
being peculiarly wealth, it may be defended on reasonable
grounds : for (1) ihe expense of the mint is very small
compared with the amount of coin turned out, and (2) the
coins produced are used by the nation, and therefore their
expensd may quite fairly be defrayed from the national
revenue. Again, as the profit on the silver coinage (owing
to circumstances to be subsequently discussed) is large,
that may be set off against the free coinage of gold. The
charge levied on coining,' if confined to the expenses in-
curred, is called brassage ; if it is anything above that cost
it is known as seigniorage, which latter term is also used
to denote both kinds of charge. The effect of seigniorage
(using the term in its more extended sense) on the value
of coins is to lower them, in fact, as Tooke has put it,
seigniorage is always a kind of debasement, unless accom-
panied with limitation.^ If the same quantity of metal be
in circulation there will be a greater number of coins, and
therefore nominal prices will be higher. It is, however,
possible that the increased prices may check the produc-
tion of the precious metals, thus making the value of the
metal higher than it would otherwise be. Whether this
will happen or not depends on the actual conditions of
production, and is incapable of being predicted. One
advantage which undoubte'dly results from a charge on
coinage is that it checks the tendency to melt coin when
exported, for where a seigniorage is imposed coins are
more valuable than the uncoined metal by the amount of
the seigniorage. It therefore becomes the interest of the
holder not to melt down the coins, as in doing so he loses
the extra value given by the coining. Another factor in
the expense of ciurency \a the loss which arises from the
wear and tear which money undergoes, and the consequent
cost of replacing the light or missing pieces. The last and
largest item is the interest on the total amount of money in
use. To take the case of England, the value of the metallic
currency is estimated at about .£1 30,000,000. The interest
* " We may take aa an example the function {which ia a monopoly
too) of coining money. . . . No one, even of those most jealous of state
interference, baa objected to this as an improper exercise of the powers
of government. " Mill, PWnc, B. v. ch. 1, § 2. But see, for objections,
H. Spencer, Social Slatia, pp. 400-402, and J. L. Shadwell, SysUm o/
Pol. Earn., p. 264.
» rooke, Hist, of Prices, L 121 sq. It is impossible, however, to
agree with Tooke that uncoined bullion would be higher in value
than coin when a seigniorage is charged on the latter. He seems tt>
ignore the fact that the value of the precious metals is partly depend-
ent on their use as currency, and that the seigniorage represents a
tax levied on the extra value resulting from the use of the metal us
money.
72Jo
MONEY
on this at 5 per cent, wouldamount to £6,500,000. This ap-
parently heavy charge is justified by the fact that it is desir-
able to have a currency possessing, or at least based on, value.
The expense of a metallic currency is, however, combined
with its weight, a strong reason for the great developments
of representative money and credit in modern times, with
the result that gold and silver are hardly ever used in large
domestic transactions, all such payments being made by
cheques, which are cleared off against one another. For a
full account of the modern organization of credit, see the
article Banking.
6. Historical Outline of Depreciations. — The earliest sy's-
tems of currency whose progressive debasements it is possible
in any degree to trace are those of the various Greek states,
though even here many details remain in obscurity. The
Uoraan currency system is comparatively better kno^vn ;
while for the medieeval currencies from the time of Charle-
magne (800 A.D.) elaborate materials are available, which
naturally increase in bulk and precision as we approach
more modern tunes. The general treatment of the history
of coins belongs to Numismatics (j.".) ; but the history
of monetary depreciations is important in connexion with
the theory of money as illustrating the value of sound
economic knowledge.
Until coinage became a state function a continued debase-
ment was impossible, since it was open to any one to refuse
the money offered in payment if it was not up to the proper
standard. When, however, coinage became a function of
government strong motives for debasement soon presented
themselves. (1) The cost of coinage falling on the state,
and being generally defrayed by a seigniorage, led to the
idea that this seigniorage could be made more profitable
by making it larger, while the existence of any deduction
veiled the injustice of a charge exceeding the expense
incurred in the operation of coining. (2) The position of
most Governments was that of debtors, and as a debasement
favoured all debtors at the expense of aU creditors it was
only natural that rulers, ignorant of the ultimately ruinous
effects of a series of debasements, should seek to relieve
themselves without exciting the odium incurred by the levy
of heavy taxes. A more pressing case than the foregoing,
and one where more justification exists, is that of a severe
social crisis, when large numbers of the community are
burdened with debt, and a depreciation of the monetary
standard seems the simplest mode of escaping from so
critical a situation. Whatever may be the inducements
to enter on the perilous course of tampering with the
monetary standard, a long experience has incontestably
proved its disastrous effects. One of the great causes of
the weakness of France during the " hundred years' war "
was the extremely debased state of its currency, and the
dread of further reductions in the value of the coins.'
Lord Maeaulay has given a graphic picture of the evils
which England suffered from its depreciated silver currency
towards the end of the 17th century.^ And a debasement
brought about by design possesses a further clement of evil
by creating a belief that similar devices will soon be again
resorted to. So manifest are the evils that result from
debasement that it may bo reasonably hoped that all civil-
ized Governments have abandoned the practice for ever ;
though, unfortunately, similar bad effects are produced by
the over-issue of inconvertible pa]Tcr currencies, and this is
still an expedient adopted under the pressure of dilliculties.
"It is proper to observe that coins may be debased in
three different ways — (1) by diminishing the quantity or
weight of the metal of a certain standard of which any coin
of a given denomination is made ; (2) by raising the
nominal value of coins of a given weight and made of a
' J. E. T. i:..:,.
- list. o/K«.j.,
Ilislorical Olcaiiings, i. p. 97.
metal of a certain standard, that is, by making them current
or legal tender at a higher rate than that at which they
passed before : (3) by lowering the standard or fineness of
the metal of which coins of a given weight and denomina-
tion are made, that is, by diminishing the quantity of pure
metal and proporti»nally increasing the quantity of alloy." '
The last of these methods is the most dangerous, since the
detection of it is more ditEcult, as it is so much easier to
discover the weight than the fineness of the metal in a coin ;
but all of them produce the same results and are adopted
for the same reason^.
Gh-cel' Dci'rcciaiioiis. — The first Jjbasoniont of coinage known tons
on good evidence is that of the Atlieuian coinage Irj- Solon in 694 B.C.*
In order to obviate the severe dii^trjss of that period in Attica, he
reduced the quantity of silver in the coins more than 25 per cent., so
that 138 new dra^h-nim (the standard .'\ thcnian coin) were only equiva-
lent to 100 pieces of the older coinage. This proceeding was*perh3ps
justified by the critical state of things previously existing, and wag a
decided success. It is probable that another debasement of the
gold coinage took place at Athens in 408 B.C. during the strain of
the Peloponnesian War, though doubts have been cast on the reality
of this debasement.' It may, however, be said that generally the
Greek cities fairly maintained the standard of money, though soliie
states were notorious for dishonesty in this respect. The existence
of an electrum coinage is no proof of a tendency to debasement,
since it was regarded as a separate substance, and issued at its cost
value, allowing for the expense of coining. As remarked before, this
comparative honesty in relation to the coinage may be partly
explained by the small extent of the Greek states, so that a debased
coinage was unable to circulate beyond the boundaries of the
issuing state. The keen perceptions of the more advanced Greek
thinkers and their teachings on this subject may have also con-
tributed to the same result.*
Soman Depreciatiojis. — The earliest Roman coinage was com-
posed of an alloy of copper (sei), and this continued unaltered
up to the time of the Fia'st Punic "U' ar. Silver was introduced in
269 B.C., the proportion between it and the older copper being
fixed at 250 : 1.* The copper cuiTency was first debased during the
Punic wars at the most critical period of the Hannibalic inva-
sion— " the Romans had debased the silver and copper coin, raised
the legal value of the silver currency more than a third, aud issued
a gold coinage far above the value of the metal." ^ Soon after this
period the copper money, whose successive debasements are recorded
by Pliny,^ seems to have been reduced to the position of a sub-
sidiary currency, so that it is not really a case of debasement of
the standard. The silver dcTuirius which at iiist was y'jd of a
Roman pound, had been debased to -^th of a pound. In 91 B.C.
a number of plated denarii were issued at the rate of one for every
seven silver pieces issued. This proceeding, which was simply for
political purposes, was proposed by Drusus, out in 84 B.C. a proposal
for calling in these plated pieces was passed, and was extremely
popular. It is probable that a slight debasement took place under
Sulla, aud one of the Cornelian laws seems to state the so-called
fiat theory of money. ^^ The denarius was lowered under Nero to
5^th of a pound, while the later period of the empire is a scene of
continual tampering with the currency. The gold aurcxts was at
fii'st -jVth of a pound, but at the time of Augustus it was only ^sth,
while under Constautine it had come to be only T^jd. The com-
parison of Hellenic with Roman monetary history seems to sho.w
that a considerable number of small states, all issuing coins, are
less likely to meddle with the standard than the mint of a single
large empire. It also proves the value of an acouaintanca with
monetary theory, if we can judge by contrasting the views of tho
Greek thinkers with those of the Roman lawyers." A few words of
caution may here be added against the danger of a careless com-
parison of values, as expressed in ancient or even mediieval money
with those of modern times. It is exti'emely hai'd to accept the
' Lord Liverpool, Coins of the Rcalvl, p. 37.
* Grote, I{ist. o/' Greece, part ii. cb. 11.
' Ik, vol. iii. p. 116, note 1.
' For a full discussion of this point see Lenormant in Conttmp.
Rev., February 1879.
' Mommsen, Uist. of Rmn. (Eng. trans.), i. p. 458.
« Tb., ii. p. 173.
» II. N., xxiiii. ch. 13.
'" Mommsen, iii. pp. 413-414 ; Lenonnant, op. cit.
** Compare, for instance, the passage previously cited from Aristotle
with the following ; — "Quia non semper nee facile coucurrebat ut, cum
tn haberes quod ego desiderarem, invicem haberem quod tu accipere
velles, electa materia est cujus publica ac perpetua sstimatio difficul-
tatibus pcriuutationum scquulitatc qu.iutitatis subvcniret ; caque
materia fornin publica percussa usiiin douiiniuuique non tatii el
(lubstAlltia prxbel qnam ex quautiutc." — Paulus, Iti'j.^ xviiL 1, 1.
MONEY
727
prices given hy any uucienc writer, Bince the varying factors neces-
sary to be estimated are so many, viz., (1) the weight of the coin,
(2) its purity, (3) the value of the monetary metal at the time,
(4) the value of the commodity sold in relation to other things,
(5) the question whether the commodity was iu its normal state as
regards supply and demand ; to all these may be added (6) the
ditlicultj- of determining whether the figured have not been altered. '
After the fall of the Western empire, the various barbarian sove-
reigns adopted silver as their principal coinage, combined with
the greatest diversity in the systems adopted. On the revival of
the empire under Charlemagne an effort was inade by him to estab-
lish a general system of currency, based on the silver pound as a
unit, and thns corresponding to the unit of weight. This system
was introduced into England, and thence into Scotland, but the
rapid decay of the Carlovingian empire prevented any uniformity
being preserved in these different countries, while the different
debasements in each produced widely divergent systems, which
will retiuire separate notice.
E.iglish Depreciations. — The first debasement undergone by the
English silver coinage was in 1300, when Edward I. reduced the
amount of metal in the coins by 1^^ per cent., or, in other words,
20 shillings and 3 pence were coined out of the Tower pound
instead of 20 shillings as previously.' This was the prelude to a
series of changes which were carried out during the next three cen-
turies, and which terminated in 1600, when the pound troy of
silver was coined into 62 shillings ; since that time the silver coinage
ias not been debased, the reduction carried out in 1816, by which
66 shillings were coined from the troy pound, being accompanied
by a limitation of its use in discharging debts to a maximum
amount of £2, as well as by the abolition of the public right of
coining silver at the mint. The period extending from 34th Henry
VIII. to 6th Edward VI. (1543-1552) has been specially noted by
Lord Liverpool as a time of peculiar interference with the fineness
of the metal.* The old proportion of 11 oz. 2 dwts. of metal to
18 dwts. of alloy, was altered to 10 oz. of metal per pound, then
to 6 oz. or one-half, 4 oz. or one-third, and finally in 1551 to 3
oz. of pure metal and 9 oz. of alloy. A tendency to reformation
began under Edward VI. , and was finally carried out under Eliza-
beth in the recoinage of 1560, which has been fully described by
Mr Fvoude.* Various proposals to depreciate the silver currency
have been made since then, and one of these, as above mentioned.
Was accepted in 1600. The most remarkable of the unsuccessful
schemes tor debasing the standard was that of Lowndes, which
was advanced in 1695, when the discussions preparatory to the
recoinage of 1696 were being carried on. Lowndes's plan was to
coin the pound troy of standard silver into 773. 6d. , thus debas-
ing it 25 per cent. Ho was resisted by Locke, who, in his Further
Coitaidtrntions concemitig Fiaising the Value of Money, contri-
buted materially to the development of monetary theory; and
the recoinage was, mainly in consequence of his efforts, in combina-
tion with those of Newton and Montague, based on thoroughly
sound principles.' - The first English gold coinage, so far as lias
been cle.irly proved, was that of 1257, in the reign of Henry III.,
wlien a small number of o:old pennies were coined at the ratio of
10 to 1 to the existing silver coins. Previously to this date the
need of gold for business transactions could not have been felt, as
the commerce of the country was necessaiily limited. It is prob-
able that for the few transactions of foreign trade a species of
gold coins issued by the Greek emperors at Constantinople, and
thence called by^aiUs, were used.* Another gold coin, known as a
fioroice, fiom the place where it was fii-st coined, was also used
after 1250. The regular series of English gold coinage begins in
1344, when Edward III. coined, in imitation of the foreign coin
just mentioned, a large number of florins «t the rate of 50 to the
f ower pound. The gold coinage was, however, for a long period a
secondary part of tho monetary system, and suffered a series of
changes, the last of which took place in 1717.' Tile present English
coinage system is regulated by the Coinage Act of 1870,' which
amends and consolidates previous Acts on the subject. Tlie schedule
to that Act, which is reproduced at p. 4S4 of the present volume,
gives full information as to existing coins, their weight, fineness,
"'remedy," &c. ^ -
Scotch pcprcci,u!ons.—The coinage of Scotland was derived from
the primitive Carlovingian system through the medium of England,
and for a long period remained the same as at first. The pressure
> As to the varioas eleraents requisite for a proper estimate of medieval
JjTices. lee Cibririo, Delia LcoHOmia Potitica del Medio Era, 1. iiu c. S,
• i The Tower pound, which was three-quarters of an or. troyless than the
troy pound, was used in England until the ISlh of Henry VIII. (15'2T), when it
WIS replaced by the troy weiglit. This should be al«'a)'s remembered in con-
sidering the precise amount of depreciation st any given time.
« Coiiu o/Ihe Sealm, ch. liii. « Hisi. o/Eiij., vii. p. !.
5 Uacaulay's account of this recoinnje. which is written in his ti-pical man-
ner, has made this episode of English monetarj- history very generally known
• Lord Liverpool, Coins of the Realm, p. 47.
' The third great English recoinage was that of tho 50H coin, which took
Vlace in 1773-1775. It is Commonly known aa the recolaage of 1774
« S3 A .;4 Vic. c 10.
under which the resonrccs of Scotland sutferea during the constant
wars with England, as well as perhaps the example of their close
ally France, led the Scottish sovei-eigns to debase their coins out of
all proportion to the English system. This was the reison for the
prohibition of Scotch coins as currency 6y tale in England, the
variation in course of time being so great that in 1600 the pound
of silver, which contained about three pounds sterling English, was
made into thirty-six pounds Scotch, the latter being thus twelve
times as much debased. After the union of the cro»-ns in 1603
no steps were taken to assimilate the two systems, which con-
tinued as before till the complete union of the two countries in 1707.'
At the latter date a complete recoinage on the basis of the English
system was canied out, thus rendering the coinage of both coun-
tries exactly similar. This most valuably reform was at first viewed
with suspicion by the Scotch people, and a large amount of the
old Scotch currency was hoarded or exported.
Irish Depreciations. — No coined money existed in Ireland before
the English invasion in 1170. The English colony, aa a matter
of course, used the same coinage as the taother-country, but on
several occasions inferior money was introduced, as being good
enough for a subject country. At the recoinage of 1560 it was pro-
posed to send the bad coins that were called in to Ireland, but to
this Elizabeth refused to assent. From 1689 to 1825 the nominal
value of the coinage was 8J per cent, higher in Ireland than in
England. In the latter year Irish money was reduced to the
English standard,* from which time the United Kingdom has pos-
sessed a perfectly uniform system oi metallic money. ■- -H
French Depreciations. — The monetaiy system established by
Charlemagne throughout his dominions soon disappeared in Italy
and the German provinces. It continued to exist in France proper.
The general state of confusion, however, and the weakness of the
central authority, led to local issues by the various feudal loi-ds.
"At the accession of Hugh Capet as many as a hundred and fifty
are said to have exercised this power. '"> The increase of the power
of the Capetian kings enabled them to restiict this freedom of
coinage, and to reserve to themselves this profitable function, the
seigniorage on the process of coining being a special branch of the
royal revenue. They were unfortunately not inclined to confine
their gains to this legitimate source. The French coinage was
recklessly debased duiing the many centuries from Philip I. (06.
1108) to Louis XV. (ob. 1774). The management of the mint
under Louis IX. was always regarded as a model for imitation,"
but even in his time the livre, originally a pound, was debased to
less than one-fourth of its primitive value. The dealings i\ith the
cunency were still more unscrupulous during the protracted wars
n-ith England, the result being that at the acces.«ion of Louis XI.
(1461), when the English had been finally expelled from France,
the livre was only about one-fifteenth of its original value. Nor
did the depreciation of the cunency rest here. The period of
something over a century, extending from 1497 to 1602, presents a
remarkable series of changes in a downward direction, no less
than nineteen depreciations having taken place, many of them
consisting of changes in the fineness of the metal.'" There is in this
respect a remarkable analogy between this epoch 01 French coinage
and the English period from 1543 to 1552.
The history of French depreciations did not terminate, as that
of the English ones did, with the close of the 16th century ; nnder
Louis XIV. the livre was only one-half of what it had been undei
Henry IV. The final Tesult was that in 1789 the livre had come
to be only one seventy-eighth of its weight in the time of Charle-
magne. At the Revolution it was converted into the franc, at
the rats of 81 livres to 80 francs." It is not, however, to be
supposed that the changes in the French currency were always
towards debasement. The terrible evils arising from the debased
coinage led to a general outcry, which in' some cases was so strong
as to force the king of the time to reform the monetary standard ;
one striking instance occun-ed in the reign of Philip IV.," whost
dealings with the currency led to his receiving the epithet of "le
faux monnoyeur."
Depreciations in other Countries. — The very brief notice of the
depreciations in the originally uniform currencies of England and
France which has just been ^vcn is sufficient to establish the
general tendency, and throws light enough on the resulting conse*
quences ; a similar course was followed in the other countries of
Europe, but the details are too unconnected to be conveniently pre-
sented. A few facts will suffice. Thus, the Gennan florin "wa«
originally a gold coin of the value of about 10 shillings of our
pre-sent money ; it is now become a silver cohi of the value of
* A survival of this older system is to be found in many charges on Irish
lands, which are reduced to English money by deducting one-thirteenth fruol
the nominal amount.
l» Hallam. iliJJle Agti, i. p. 206.
11 Stephen, Ucluret on French History, I. p. 459.^
12 Tooke and Newniarch, Hisr. of Prices, vol. tL' p.' 374. The views there
given are based on those of M. Levasseur, who had specially studied the
question.
13 The silver franc was made to weigh exactly & grammtt,
" Stephen, i»cl. on Tmch Uin., i. p. 481
y
728
MONEY
ci:Iy 20J. " ' Similar dejireciations took place in the cases of the
Sj|anish mamvcdi and ' > Portuguese rei. At the present these
coins are so suborilinate, ,\-here they have not been abolished, aa to
jiossess little practical imprest.
It is well to notice before concluding the question of
depreciations tLat it is the poorer classes who especially
suffer from a change in the coinage. The reasons of this
are very plain, for from their ignorajice they are less able to
understand the nature of the alteration, and, even if it were
not so, the absence of available resources places them at a
disadvantage in comparison with others. Masters and
dealers are quick to discount — so to speak — the nominal
value of the depreciated money, and prices are much more
speedily adjusted to the new state than wages, so that it
may be confidently asserted that a debased coinage is
especially injurious to the more helpless classes of society.
The same remark appUes to an over-issue of inconvertible
i Daper.^
7. Economic Aspects of the Production of the Precious
jyletah. — In considering various monetary questions it is
essential to have some acquaintance with the economic
aspects of the production of gold and silver. The technical
matters connected with the processes of preparing those
metab for use aro to be found in the articles Gold and
Silver (q.v.). The first point to which we will here direct
attention is the field over which production extends.
At one time or other these two metals have been found
in every continent. Asia Minor in early times possessed
its gold fields, or rather auriferous sands.^ Ceylon also
undoubtedly contained gold mines. China and India
both produced silver to a considerable extent. Egyptian
remains show that gold was commonly known in that
country, probably procured from Nubia and Abyssinia.
On the opposite side of Africa, too, the name of Gold
Coast shows that that metal was thence exported. Neither
Asia nor Africa, however, has been the main contributor
to the stock of money in more modem times. The
mines of Lauriura in Attica were a source of supply to
the Greeks, and were worked as a state monopoly. At an
earlier date the Babylonian and Assyrian empires had
each large accumulated stores of gold. The Phoenician
importations of gold from the Red Sea coasts (Ophir) are
kno-n-n from Scripture.^ The Persian kings from the time
of Darius levied tribute on all their provinces, — in gold
from India, in silver from the remaining districts ; and
the larger part of this was stored up in the royal treasuries.*
This tendency of sovereigns to accumulate had all through
ancient history important eflTects on the economic structure
of society. At present it is quite natural to assume that the
materials of money are distributed by means of international
trade, and tend to keep at an equal level all the world
over, — an assumption which is in general well grounded,
though an important exception exists. Ancient history
presents a widely different set of forces in operation. Gold
and silver were produced by slaves under the pressure of
fear, and were drawn towards the ruling parts of the .great
empires ; in a word, war, not commerce, was the distribut-
ing agency. From thi-i condition of affairs it is easy to see
tliat whatever may be the reasons for assigning to cost of
production a potent iiiducuce over the value of money in
modem times (and grounds have been already advanced
for the belief that this influence has been exaggerated), no
such reasons then existed. The production of the precious
' Lord Lirerpool, Coins of the Realm, p. 125.
* Readers requiring full details on the subject of the various currency
changes may coaault Lcnormant, Monnaie dans V AntiquiU, for
ancient times ; Lord Liverpool, Coin* of the Realm, for England ; and
the works of Le Blanc and Paiicton for France.
' The Pactolua in Lydia was widely famed for its " golden sands."
•* 1 Kings ii. 23.
^ See Horodotvu, Ui. c. £6 ; also Grots, IliJ., iv. pp. 162 si.
metals waa carried on, as the great buildings and other
works of those periods, on non-economic grounds, and
therefore produced quite different effects. The whole his-
tory of the Persian monarchy to its overthrow by Alexander
(330 B.C.) shows that the mass of the precious metals
hoarded up continued constantly to increase. On the cap-
ture of Persepolis by the Grecian army an enormous treasure
was found there, some estimates placing it as high as
120,000 talents of gold and silver (£27,600,000).° All
the temples, too; were receptacles for the precious metals, so
that the stock accumidated at about 300 B.C. must have
been very great. The only causes which tended to diminish
the store were the losses arising from wars, when the various
treasuries were liable to be plundered and their contents dis-
persed.^ There was therefore a more imequal distribution of
the material of money than at present. The growth of the
Eoman dominion led to important results, since under their
rule the Spanish mines were developed and became a leading
source of supply. The great masses of treasm-e set towards
Rome, so that it became the monetary centre of the world.
The overthrow of the Republican govenmient and the
peace which followed also affected the conditions of pro-
duction. The inefficiency of the Roman administration
made it advantageous to let out the mines to farmers, who
. orked them in a wasteful and improvident manner, while
the supply of slaves was reduced, thus depriving the lessees
of their principal agency for carrying on production. The
result was a continuous decline in the store of money. Mr
Jacob has made an attempt to estimate the amount at the
death of Augustus (14 a.d.), and he arrives at the conclu-
sion that it was £358,000,000.' Without placing much
value on this necessarily conjectural estimate, it is safe to
a.ssume that this period marked the hisbest point of accu-
mulation.
The succeeding centtiries exhibit a steady decline, though
it is of course impossible to attach any value to even the
most carefully-guarded numerical estimates. The pheno-
menon which has since so often attracted notice — the drain
of the precious metals to the East — began at this time,
and was a subject of complaint to the Roman writers,*
whUe the stock of gold and silver being thrown into
more general circulation suffered more from abrasion, and
was more likely to be lost than when stored up in the
royal treasure-houses and temples. These causes tended
to depress the scale of prices, while the barbarian Inva-
sions produced a strong effect on the supply by drawling
off the mining population and damaging the various erec-
tions used for working the mines. The conjectural esti-
mate is, that about 800 a.d. the total supply had been
reduced to £33,000,000 (or about one-eleventh of what
it had been at the death of Augustus).'" A new j*riod
in the historj' of gold and silver production may be fixed
at this date. The Moors, now firmly established in
Spain, began to reopen the mines in that country which
had been allowed to fall into disuse. Other European
mines also were opened." The international system of
currency based on the pound of silver as a unit which was
introduced by Charlemagne must have tended to economize
the wear of the metals. We may therefore conclude that
from this date (800 A.D.) the supply was suflScient to coun-
• Grote, xi. p. 409, note 3.
' A commercial agency which existed for the distribution of goU
and silver was the Pb<en- ' system of t'Tiding, which extended all
over the Mediterranean.
* Jacob, Production and Con$vmption of the Precious Metate^ i.
p. 224
» See Pliny, U. If., xii. c. 18. " Jacob, L p. 235.
" It was at this time that the most productive European mines
were discovci-ed, namely, those of Saxony and the Hara Mountains, aa
well as the .\ustrian mules ■which were the chief sources of sapply
during the Middle .ig-.:u
MONEY
729
tera't the l«ss by wear and exportation,' and accordingly
regard the metallic supjily as axed in antount until the
next change in the conditions of production; which was
the res'.ilt of the discovery of America. Though 1492 is
the dato of the first lauding, yet for some time no im-
portant additions wore made to the supply of n.oney.
The conquest of Mexico (1519) gave opportunities of
working the silver mines of that country, while the first
mines of Ciiili and Peru were almost simultaneously
discovered, and in 1545 those of Potcsi were laid open.
From this latter date we may regard the American supply
Ta^le I. — EstiiiiaUd produelim of gold and siher/roin 1493.
1
....
Amonst in Kilos.
Valui! In Millions
of Fran(rs.
Ratio of
Value of
Period.
Teai-s.
0-5M to
Ooia.
Silver.
Gold.
SOver.
SUvcr.
1493-IJ20
28
162,400
1,316.000
560
292
lis
1521-1544
24
171,800
2.105,000
592
481
11-2
154i-15S»
SO
273,000
io,9,«,oao
940
2.439
11-5
1581-1000
20
147,600
8,.>i78,000
iOS
\M-2
11-9
)601-K20
20
170,400
8,,,:<ooo
587
l.SSO
13-0
1621-1(140
20
166,000
7,S72.0«0
672
1,749
13-4
1C41-1000
20
175,400
7,526,000
601
1,628
ue
1(161-1080
20
185,200
6,. 40.000
638 ■
1,498
14-7
1081-1700
20
215,300
0,S38.000
742 .
1,500
15-0
1701-1720
20
250,400
7.112.000
883 ,
1,580
15-2
, 1721-1740
20
881.000
8..124,000
1.314
1,9!C
16-1
1741-1760
20
492.200
lO.AS.OOO
1,095 1
2,370
14-8
17Cl-'780
'.0
4i4,:Ki
13.115-..000
1.436 1
2,900
14-1
1781-1800
20
35^600
17..-81,000
1,228 •
3,906
15-1
1801-lSlO
10
177,800
8,1M2,000
612 .
1,087
15-6
ISll-lSiO
10
114,400
6,408,000
394 1
1,202
15-5
182I-1S:10
10
142,200
4,ooi.ooo
490 1
1,023
15-5
18:11-1840
10
202,900
5,961.000
099
1,325
15-7
1841-1850
10
6^7.600
7.804.000
1.881 ,
1,734
15-8
1851-1855
6
9S7,6JI
4,431.000
3,402
985
15-4
1850-1860
i
1,030,000
4..,w,(i00
3,549
l.OOG
15-3
18iil-18«5
5
925,000
5,506.0.-0
3.188 :
1,223
154
16.-.(>-1870
5
959,500
0.005.000
3,305
1.488
U-6
18T1-1875
853.400
9,847.000
2,040 ;
2.18?
16-0
1876
171.700
2.305.000
59! J,
62S-5
17-8
1877
162,800
2.42S.O00
629-8,
539-5
1719
1878
183.700
i.oli^.OOO
632-6 1
578-3
17-96
, 1876
156,900
2,557.000
640-3:
508-2
18-39
1876-1879
4
695,100
9,953.000
2,394 1
2,211
17-40
1 149S-18.i0
358
4,752,100
149,828.000
16.308
33,292
14 -Oi
1851-1879
29
5,451,200
40,;'57.000
18,778
9,101
15-85
! 149S-1879
387
10,203,300
190.765,000
35,144
42,393
as an influential factor in the matter,^ and look upon the
stock of money as increasing. The annual addition to the
store of money has been estimated as £2,100,000 for the
period from 1545 to 1600. At this date the Brazilian
supply began. The course of distribution of these fresh
masses of the precious metals is an interesting point,
which has been studied by Jlr Cliffe Leslie.^ The flow of
the new supplies was first towards Spain and Portugal, and
from thence they passed to the larger commercial centres
of the other European countries, the effect being that
prices were raised in and aboQt the chief towns, while the
value of money in the country districts remiined unaltered.
The additions to the supply of both gold and silver during
the two centuries 1600-1600 continued to be very consider-
able ; but, if Adam Smith's view be correct, the full efl'ect
on prices was produced by 1640,'' and the increased amount
of money was from that time counterbalanced by the wider
extension of trade.^ At the commencement of this cen-
tury, the annual production of gold has been estimated
as being from £2,500,000 to £3,000,000. The year 1S09
ieems to mark an epoch in the production of these metals,
since the outbreak of the revolts of the various Spanish
' Jai-ob, i. p. 311.
- Adi.ta Smith asjtnmes 1570 an the date when prices were affectcfl
in En5l.-\':.l, Wi^ltli of Xatims. p. 88. Huraboldt estimated the total
prodni-tion (1492-16451 as being about £17,000,000; but see Table
I., which contains Dr Sotbeer's estimates, based oa the best available
data.
• J^sfvt IK Fcl. and Uor. Phil., Essay xx.
«■ ICjoi/A or Xdtimis. p. 88.
• The total production is ir>ii!rhly computed at over £1,200,000,000 I
\o* the two oeuturiea 1600-1800 j but see Table I. f(x i>:ore precise '
ctttoiateff. I
dependencies in South America tended to check the usual
supply from those countries, and- a marked increase in the'
value of money was the consequence. Duiing the period
1809-1849 the value of gold and silver rose Xr about two
and a half times their former level, notwithstanding fresh
discoveries in Asiatic Eussia.° The annual yield in 1 849 was
estimated at £8,000,000. The next important da,te for
fiur present purpose is the year 1848, when the Calif orniaii
mines were opened, while in IS.tI the Australian discoveries
took place. By these events an enormous mass of gold
was added to the world's supply. The most careful
estimates fix the addition during the years 1851-1871 at
£500,000,000, or an amount nearly equal to the former
stock in existence. The problems r^.iaocl by this phen(jJ
menon have received the most careful study by several
distinguished economists,' to whose writings those desiring
more extensive information may refer. The main features of
interest may be briefly summed up.. (1) The additional
supi>ly wa.<i almost entirely of ffoUl, thus tending to produce
a distinction between the two p:-inci]ial monetary metal^
and an alteration in the currency of bimetallic coiuitriesj
Under this influence France, from being a silver-u.sing,'
became a gold-using, country. (2) The contempora-j
neous development of the Continental railway systems,
and the partial adoption of free trade, with the con-^
sequent facilities for freer circulation of commodities, led
to the course of distribution being difierent from that
of the 16th century. The more backward districts wer^
the principal gainers, and a more general equalization of
prices combined with a slight elevation in value was the
outcome. (2) The increased supply of gold rendered a
general currency reform possible, and made :be use of a gold
monometallic standard appear feasible. The movements
for currency reform, as will be seen, all arose after these
discoveries. (4) The change in the value of money, which'
may for the period 1849-1869 be fixed at 20 per cent.J
enabled a general increase of wages to be carried out, thus
improving the condition of the classes living on manua-l
labour. It may be added that the difliculty of tracing the
effects of this great addition to the money stock is a most
striking proof of the complexity of modem economic
development. (5) The last point to be noticed is the very
small influence exercised on the value of silver by the new
gold." Hardly had the gold discoveries of 1848-1851
ceased to jiroduce a decided effect when new sih'er mines
of unusual fertility came into working. During the period
immediately succeeding the gold discoveries the produc-
tion of silver remained at an annual amount of from
£8,000,000 to £9,000,000. This amount suddcnlv,
about 1870, increased to £15,000,000,'" and remained i<'
that amount for tlie next five years. More than half c5
the supply came from new mines oi)ened in Nevadp
This increased supply was accompanied by a marke,-'
depreciation :» tlie j;olJ pi ice of silver, though the price.s
of commodities in countries having a silver standard did
not rise. The result of the close investigations to which
all aspects of the question were subjected was to show
that the increased pr(3duction of silver was only a minor
element in causing its depreciation. The policy pursued
by various states — viz., (1) Glrmany and the Scandinavian
• Tlie Russian supply became important after 1823. ^
" The following may be specially consulted : — Chev-ilier. DepT'ciatioa
of Gold (traus. by Cobden) ; Tooke and Newmarch, Uist. of Prktt,
vol. vi.,fp. 135-236 (Part vii.); aiticle "Precious Metals," .SJK-y. Dril.
{8th E>1.) ; J. E. Diirnes, Ksmya in Pol. Econ., pp. 1-165; T. B. C.
Leslie, Essoya, pp. 264-374 ; W. S. Jevons, Serious pidl in the Valxtt
of Gold.
' The price of silver in Loudon rose from 59Jd. per oz. to 62M. per
02., or 25d. per oz. — that ia, only 3 to 4 per cenu
» See P.eport of Select Committee on the Silver Qlfestiou, 1876 ; tuii
for another estimate see Table L
730
MONEY
states in adopting a single gold standard, (2) the
•eountiies compoaing tlie Latin Union in limiting the
■coinage of silver, (3) the Indian Government by
adopting a new method of drawing bills — proved to be the
really influential causes for the decline in the value of
silver as contrasted with gold.^
Before closing this notice of the economical aspects of gold and
silver production, the consumption of those metals must be con-
sidered. It may be classed roughly under three heads, viz., (1)
their use as merchandise, (2) their use as money, (3) the export to
the East. With regard to the first of these, while it is impossible
to give precise data, it may be still held with some confidence that
the demand for this purpose tends, after society has passed a certain
not very advanced stage, to declijie. The desire for personal adorn-
ment is with most civilized persons not a strong one. It is, so far
as it exists, gratified by other articles than those made of silver or
gold. Their use as manufactured goods continues to be large, and
is one of the principal forms of use at present. The second head
with which we have here to deal is the one by which prices are
affected. The laws regulating the value of the metals as money
have been considered above, p. 721, the primary one being "that
the value of money varies inversely as its quantity multiplied by
its efficiency," though this proposition needs limitation and explana-
tion. Under the tliird head a remarkable exception occurs to the
general theory of the tendency to equal diffusion of the precious
metals. For a peiiod extending over nearly 2000 years the move-
ment of silver fiom West to East has been noticed. Humboldt has
made the ingenious remark that these metals move in the opposite
direction to civilization, and history bears out his view. During
the Middle Ages the chief Eastern products used in Europe were
silks and spices, and to pay for these commodities silver was sent
from Europe. The discover}- of the passage round the Cape of
Good Hope increased the Eastern trade, and added to the drain of
silver. Humboldt and Sotbeer have given copious details. In
more recent times the flow has continued, the amount of silver
■which passed to Asia by the Isthmus of Suez during the twelve
years from 1S51 to 1862 being £110,000,000.2 There are two points
requiring some further notice with reference to the form and the
reason for this drain. SUver is the metal which is exported from
Europe, since gold is not used for currency puriioses in the East,
and even as merchandise silver possesses a higher relative value
than it does in Europe. Those European countries that had a
double standard were the natural source of supply for exportation,
their silver currency being replaced by gold. The unceasing drain
of the precious metals to the East may further be explained by the
fact that the greater part of the new metal is used for ornamental
aiid not for currency purposes, and thus the demand is not checked
by a rise of prices. Another reason, not generally noticed, is that
Eastern prices are very much influenced by custom, and thus de
not depend on supply and demand. But it is this tendency of an
increased quantity of money to raise prices which forms the basis
•of the economical theory of the distribution of the precious metals.^
This explains the otherwise unaccountable phenomenon of a con-
tinual drain of the money material towards those countries where
custom has remained most powerful in regard to commercial trans-
actions, or, in other words, the bacluvard countries of India and
China.
One of the technical features of the profluction of the precious
metals may sometimes produce remarkable economic effects, —
Tiamely, the fact that gold is generally found near the surface, while
■iilver is obtained by deep mining. It follows from this that the
production of the farmer metal depends more on accidental circum-
stances, while the production of silver is affected chiefly by the
f.tate of mechanical skill. In the Nevada mines gold and silver
are- found together, and their value in a given mass is nearly equal.
8. Miscellaneous Questions regarding Metallic Money. —
The recent discussions of matters relating to currency, and
the increased intercourse among the more advanced nations,
have led to the raising of some questions with regard to
the proper constitution of monetary systems. Each country
possessing any claim to enKghtenment has directed its
attention to its o^vn monetary arrangements, and compared
them with those of others, while the effect which the cur-
rency system of any nation exercises on its neighbours leads
1o the exciting of a lively interest in its monetary legisla-
tion. The principal problems may be summed up under
' See, for details, the Report of Mr Goschen's Committee, 1876, and
■\V. Bagehot, Papers on the Drprmntwn of Silver.
' See A. SStbeer in the vierleljahrscilr. f\ir rMmfirlhsch., iii.,
i36S.
' See Ricardo, Principles of Pol. Econ., p. 79 {ed. M'CuUoch).
three heads: (1) The proper standard to use, the discussion
of which in practice turns on the comparative merits of a
single standard of gold or silver and of a double standard
of gold and silver at a fixed ratio ; (2) the system of sub-
dividing the currency, which is generally discussed under
the title of proposals for decimal coinage ; (3) proposals
made in many quarters to assimilate the various currency
systems of the world. These take one of two forms.
It is either desired that a group of nations shall assimilate
their currencies, in which case the coinage may be called an
international one ; or a wider view is taken, and a single
system is advocated for all states. This may be styled
universal coinage. The question of the proper standard
may be deferred for the present, as it is of a more complex
nature than the others. Before discussing even the simpler
of these questions it is desirable to state some elementary
facts involved in all such points. Every currency system
must be based on a standard unit of value which consists
of a " fixed quantity of some concrete substance defined by
reference to the units of weight or space." Thus the
English unit is the pound, which consists of a definite
quantity of gold (123-27447 grs. standard fineness), while
the French unit is the franc (composed of 5 grammes of
silver Aths fine). It is not, however, necessary that the
standard unit shall be a coin. All that is needful is that
the current coins shall be multiples or submidtiples of the
unit, or at all events easily reducible to it. The Portu-
guese rei is too small to be coiiied, and the pound of silver
which formed the unit of the early French and English
currency was too large. Distinct from both the actual
coins and the unit of value is the moyiey of account, though
in practice it is usually identical with one of them. In
Russia in early times the rouble was an imaginary money
of account not coined, while the copper copeck was the unit
of value. Another distinction must be pointed out, namely,
that between standard and token money, the former being
of the same value as the metal it is made of, while the latter
is rated kl a nominal value higher than that of its material i
The silver and copper coins in England and the smaller
silver coins in the Latin Union are merely tokens, being in
the case of the English silver coins about 30 per cent, below
their nominal value. The French coins are of inferior
fineness (835 per 1000). Token coins are only admissible
in small payments, as otherwise — in accordance with an ele-
mentary principle to be presently explained — the standard
coins would be driven out of circulation. The maxirauni
amount in payment for which they are legal tender is in
England 40s. One of the functions of money being to
afford a standard for estimating deferred payments,^ it
is generally used as the means of discharging obligations
when they become due, and in this aspect is styled leaal
tender. The principal coinage of any country is legal tender
to an unlimited amount, and, when oflfered, discharges any
pecuniary obligation. It is only the standard coinage which
possesses this property, or rather the standard coinage is
that which does possess it.
In discussing monetary questions it is also important to
remember that a metallic currency has to circulate among
the most diverse classes of society, and must he suited to
the wants, and even to the prejudices, of the population
using it. Many curious instances of the preference of a
community for some particular coin couldbe given. The
Austrian Maria Theresa dollar is a special favourite on the
coast of Africa, and is still coined exactly as it was in 1780.
The inhabitants of California refused to accept the green-
backs issued during the American civil war, and conse-
quently gold was always used in payments in that State.
Many apparently well-devised reforms have miscarried
See p. 720, abov
M 0 W E Y
731
vwing to £belia1>it3 of the people not having been attended
to. Some Avritcrs have, however, misconceived the prin-
ciples of currency ar.d extended tLia influence to cases
where it does not ;.lip!y. Tims it has been sought to explain
the adoption of gold as the principal Eni;iis.h coinage after
1696 by assuming that the English deliberately preferred
that metal.' The fact of different nations possessing dif-
ferent currencies, as the prevalence of gold in England and
of silver in France during the 18th century, is to be other-
wise accounted for. The great mass of a population, it is
true, take and give money without particularly observing
it. It is enough if the coin conforms to the usual type.
There exists, however, in all mercantile communities a class
of dealers in money ^ who make a profit by selecting the
best coins for exportation, or, if two metals are in conctirrent
use, the coins of that metal which is undervalued in the
proportion fixed. The mode in which self-interest thus
■operates produces an effect which may be briefly formulated
by saying that bad money drives out good money. It is
often now called " Gresham's law," from a former master of
the English mint,^ who observed it. The illustrations of
its working are numerous. Under its action the gold which
■was overvalued relatively to silver in England in 1696
became the main English coinage, as above stated. And
in order to meet the want of silver coins. Sir I. Newton
advocated, and secured, the reduction of the guinea from
21s. 6d. to 21s. The exportation of metallic money when
an over-issue of inconvertible paper takes place is another
case of the theorem. By means of this principle we can
easily explain the tendency of currency to depreciation, for
when once, either by wear or by the issue of inferior coins,
■a, currency has become debased, no reformation is possible
unless the debased coins are removed from circulation, as
otherwise they will be preferred for payments by dealers,
and wiU not be melted down or exported. All demands for
foreign trade will be met from the best part of the coinage.
An argument in favour of state coinage has been founded
on Gresham's law. It is argued that private coinage
would lead to the issue of depreciated money.* It is,
however, overlooked in this argument that the action of
the law arises from the fact that the depreciated ciurency
is legal tender ; were it not so, coins less than the proper
weight would be at once rejected. It may be added that
Greek monetary history bears out this view.'
Having disposed of these elementary questions, the
general groups into which all currency systems fall may now
be stated. The simplest form of currency seems to be that
in which the state coins ingots ,of different metals, and
allows them to circulate freely, without any ratio being
fixed. This, which is the lowest form of currency proper,'
has arisen in malny countries through the introduction of
coins of various other nations. Turkey is a European
example. Many of the South American republics possess
a currency of this description. A theoretical form of this
system has been advocated in France. It is proposed to
issue coins of one, two, five, and ten grammes of gold, and
to allow the present silver coins which are multiples of the
gramme to circulate along with them. The difficulties of
this plan are so obvious that there is no likelihood of its
being adopted. The arguments in its favour are of little
' R. Giffen, Etsays in Fiiianct, p. 303.
^ The Jewish aud Lombard niercliauts discharged this function in
the medioival period ; Hallam, Middle Ages, iii, p. 369, note t.
' Aristophanes {Ran. 719-733) appears to recognize tliis principle.
Orote (vol. iii. 116 note) has misunderstood him, aud seems to deny
"the principle stated.
* Jevons, .Voiiei/, p. 82. • See p. 726, above.
' In his discussion of this subject Prof. Jevons, on whose excellent
■work much of Ibis section is based, mentions currency by weight as
th« simplest form, but it is hardly correct to regard this as a currency
•jatem ; it is rither a primitive stage, closely akin to bartor.
force, sijice it is hardly correct to contend that it is a
natural system, when it has never been ivillingly adopted by
any country. The next system to be noticed is that of a
single metal being fixed as legal tender. This in early
times is the really natural arrangement, and has been
widely adopted. It is needless to recapitulate the instances
which have already been given in dealing with other
matters. There is, however, a difficulty which soon arises
under this system. If the metal chosen is not very
valuable, it is toe cimibrous for large payments ; if, on the
other hand, it possesses a high value, it is hard to coin
pieces suitable for small transactions. Thus, even silver
would be too bulky for such payments as frequently occur.
£100 in silver at its present value would weigh nearly 40
ft), while it would be impossible to coin gold pieces of
the value of a penny or even a shilling. This system thus
naturally leads to the use of other metals besides the
standard one, and when the state fixes the ratio between
the; '. metals a new system has come into existence, which
has oeen called the inultiple tender system. In it the
ratios between the metals are fixed, either once for all, or
until changed by state authority. This system was in
force in England from 1257 (or rather 1344) to 1664,
the ratio between gold and silver being fixed from time to
time by proclamation. France, too, adopted it during the
Revolution, the ratio of 15 J to 1 being that fixeci between
gold and silver. The fluctuation of currencies arranged
on this method, o\ving to the action of Gresham's law, has
led in England and Germany to a modified sj'sten, which
seeks to combine any advantages of the multiple standard
with the principle of the single standard. By this method
one metal is fixed as the principal legal tender, while the
smaller coins are made of a less valuable material, and
circulated at a nominal value somewhat above their real
one, or, in other words, as token coins, but they are only
legal tender to a limited amount. This has been called
the composite legal tender system.'
For further details reference may be made to Tables IT. and III.,
and the notes appended. Every currency system requires the exist-
ence of subsidiaiy coins, and, as stated before, this want is mi:t by using
a less valuable metal, generally silver, and for smaller payments
copper or bronze. But, apart from the question of the taaterial of
the smaller coins, it is important to determine the best rat .o between
them. The simplest of all would be the binary. In it each coin
would be the half of the next highest one, and double the one imme-
diately below it. Nothing, apparently, is plainer or simpler than
this scale, but the objection to it is the gi-eat number of coins that
would be required, as well as the want of conformity mth the
general arithmetical scale. In a modified form it does prevail in
many countries. Thus in England we have the penny, h&lf-pcnny,
&i\d. farthing. At a higher stage we have the Jlorin, shilling, six-
penny piece, and threepenny piece, and, again, the sover:ign, half-
sovereig^i, fvC'Shilling piece,^ and half-crown. The coiniiges of the
Latin and Scandinavian Unions, as also those of Germaiy and the
United States, have several binary series in their coins.* There is,
however, no completely binary system known. The old English
soale was partly duodecivuil, and the argiiments in favoiir of this
aiTangement are by no means weak. At present the shilling is
duodecimally divided. It is urged in favour of this scale that the
main divisions of time (year and month, day and hoxi, are duo-
decimally related, and that time is one of the elements in all
questions of value. ^* Another argument is tliat 12 is capable of
being resolved into several factors (2 aud 6, 3 and 4), a ad therefore
' This system came into existence in England accident:illy, through
silver being overv.ilued by the mint regulations, but i".s theoretical
basis was given by the often-quoted worlc of T/Ord Liviirpool, Coins
of the Realm (1805), which contains even now the best eiplanation of
its principles.
^ This piece is now almosv extinct.
• For ■ instance, the 20-fraiic, lO-franc, and 5-fran(; pieces, and,
again, 2-franc, l-franc, and 60-centime pieces in France, he. ; 20-kroner
and io-krouer pieces, and 4-kroner, 2-kroner, 1-kronj, 50-6re, and
25-(;re pieces in Denmark, &c. ; 20-, 10-, and 5-mark piec.'s, and 2-mark,
1-niark, and 50-pfennige pieces in Germany ; while th'! tJnited St-itts
have eagle, half-eagle, and quarter-eagle, and also dol ar, half-doUar,
and quarter-dollar.
'" See S. L.ning. Kotes of a Traveller, pp. 57-59
1732
MONEY
enables & large series of coins to be formed.^ The main reason,
liowover, for the adoption of a duodecimal system appears to have
been tho preference for the number 12 so frequently sliowu by early
sooictics ; thus, amon^ the Semitic races, the Jews were organized
in 12 tribes, and in Italy the Etruscan league consisted of two
j,Toups, each of 12 cities. In connexion with this it may be noted
that a duodecimal system of currency prevailed south of the Apen-
nines. At Rome the as was divided into 12 uncim. The modern
tendency, however, has been to adopt a decimal scale. This method
of notation, which is found very widely in use amon-^ savage tribes,
is undoubtedly derived from the ten' lingers of the human hands.
Though the base 10 is not so convenient as 12, it is firmly established
as tijo only system of counting, and is in process of extension to
1 iT. R. SrCulloch m Ency. Brit., art. "Money," voL xv. p. 431 (Sthed.).
weighing and measuring.* For the purposes of currency this scalff
is not very convenient, as 10 can be only resolved into two factors
(2 and 5), and one of these is a rather liigh number. This dis-
advantage has i-etaixled the adoption of decimal coinage, and is the
base of the objections made to it. It has been contended that it is
unsuitable for small purchased, and for such fractions as one-third,*
France adopted the decimal system of coinage in 1799, and it has
now extcadcd over all the countries of the Latin Union (see Table
II.). It is also in use in Germany, Denmark, Sweden and Non\-ay,
the Netlierlands, and Finland, as well as in the United States. But
none of these countries has a decimal coinage piu-e and simple. In-
'Tlic Coinage Systems of CoiUi-nental Europe, exhibiting the gold ajid silver coins, their weight, Jl-nenes^, remedy, and
approximate value in English and United States motley.
Rein.
Appro:(iniate
Rem.
Approicimate
i
li
p. 1000
Moiicyjalae.
i
Is
p. 1000
Money Value.
Coins.
1
1
1
4J
1
1
Coins.
1
S a
n
i
^
1§
II
Si
~
-
AUSTRIA.HUN0AEV-1_
& s. d.
0 c.
Netherlands 6—
£ s. d.
i c
100 KreiitzcT 8 Gulden piece
Gold
6-45161
900-
12-
2-6
0 16 10
3 86
100 Ctnls = 1 10 Gollder piece
Gold
6-730
900-
1-6
2-
0 16 6
4 2
= \aiiUitn 4
3-22530
900-
2-
2-5
0 7 11
1 93
GuiUcT. 6
3-31J0
900-
1-5
2-
0 8 3
2 1
2 >, >,
Silver 24 ■6914
900-
2-
2-5
0 3 11
0 96
2!
Silver
25-
945-
2-6
2-5
0 4 2
1 0
J
,,
12-3457
900-
2-
2-5
0 1 llj 0 48
I
jj
10-
945-
2-5
2-510 1 8-1
2-5J6 0 10
0 40
SO Kreutzer 11
J,
5-3419
520-
2-
2-6
0 0 6J 0 12
{
6-
945-
2-5
0 20
2-666
500-
2-
2-5
0 0 4j 0 ID
25 Cents
3-575
640-
2-5
2-5
0 0 5
0 10
10 „
1-666
400-
2-
2-5
0 0 2g 0 5
10 „
5
1-400
0-C85
640-
640-
.-5
2-5
2-5
J -5
0 0 2
0 0 1
0 4
0 2
Beloicm- See France.
NoEWiT. See Denmark.
Portugal*—
Denmark 9—
1000 Reis = l Crovm or $10-000
Gold
17-735
916-666
2-
2-
2 4 5
10 80
,100t^e = l 20 Kroner piece
Gold
8-9C0572
900-
1-5
1-6
12 1 6 30
Milrci. Half-crown or $5 000
8-867
916-666
2-
2-
1 2 21
5 40
Krone, 10
4-4S02S6
900-
1-6
2-
0 11 01 2 68
One-fifth Crown or §2 OOO
3-647
910-666
2-
2-
0 8 10
2 16
2
Silver
15-000
800-
3-
3-
0 2 23 0 63
One-tenth Cjown or $1-000
1-773
916-666
2-
2-
0 4 6
1 8
1 R'one „
50 Ore piece
7-SOO
5 000
soo-
600-
3-
3-
3-
3-
0 1 Ij 0 27
0 0 6j 0 13
SOORele
Silver
12-500
916-666
2-
3-
0 2 2)
0 64
40
4-00O
600-
3-
3-
0 0 6J 0 10
200 ,
5-000
916-666
2-
3-
0 0 lOj
0 21
25
2-420
600-
3-
3-
0 0 s! 0 6J
100
2-600
916-666
2-
3-
0 0 5j
0 11
10
1-450
400-
3-
3-
0 0 IJ 0 2)
60
RouuANiA. See France.
-"
1-250
916-666
2-
3-
0 0 2i
0 i
Fj<Al.CE<
loo (Untlmes 100 Franc piece
Russia •V—
Gold
32-25806
000-
2-
1-
3 19 SJ 19 30
100 Copeck3 Imperial or
= 1 franc. 60
"
16-1 2903
900-
2-
1-
1 19 7J
9 65
= 1 Souble. 10 Rouble piece
Gold
13-088
916-666
nil
2-
1 11 8
T 72
20
6-45161
900-
2-
0 15 10
3 86
Half Imperial or
10
^^
3-225S0
900-
2-
0 7 11
1 93
5 Rouble piece
J
6-544
916-666
2-
0 13 10
3 8&
6
1-61290
900-
2-
3-
0 S llj
0 96
3
„
S-926
916-666
2-
0 9 6
2 81
5
Silver
25-
900-
3-
3-
0 3 11)
0 96
1
Silver
20-7315
863-056
!:
0 3 2
0 77
2
10-
835-
3-
5-
0 17
0 33
)
10-3660
868-056
0 1 7
0 38
1 ..
5-
835'
3-
5-
0 0 ey 0 19 1
0 0 4| 0 10
1
5-183
668-056
2-
0 0 9)
0 19
60Ceniiines. ..
2-6
835-
20 Copecks
4-146
760-0
2-
0 0 7i
0 15 1
20
1-
835-
0 0 2
0 4
10
6 ,
2-073
1-037
"60-0
750-0
•J
2-
2-
0 0 Sj
0 0 2
0 7
0 4
Oeiis.a><t«_
Seevia. Bee France.
Spain. 3 Bee France.
100 FJcnni^i 20 Mark piece . .
Gold
7-964954
900-
0 19 7
4 76
= \MaTL 10
5
3-9S2477
1-991239
900-
900-
0 9 91
0 4 lOJ
2 38
.1 19
Sweden. See Denmark.
SWITZEELAND. SeeF?.'NCE.
rURKEY'9-
100 Pimlris MedjidieorLira
I ■■ ■■
Silver
B7-7777
900-
0 4 lOJ
1 19
Gold
7-216
916-666
2-
2-
0 13 0
4 40
u-iiii
900-
0 1 llj
0 48
= 1 Medjtdtt. J
3-608
916-666
2-
2-
0 9 0
2 JO
1
5-5555
900-
0 0 llj
0 24
i
1-804
916-660
2-
J.
Q 4 e
1 10
60 Pfennige
2-7777
900-
0 0 6
0 12
20
1-iiii
900-
0 0 2)
0 6
20 Piastres ....
10
5
Silver
24-055
lJ-027
6-013
830-
630-
630-
3-
3-
s-
3-
3-
!-
0 S V
0 1 9)
0 0 10(
0 88
0 44
0 22
Greece.* B«e Frasce.
2
*[
2-405 630-
3-
3-
0 0 4
0 9
Italy. Bee France.
1
1-202 ;630-
3-
3-
0 0 2
0 i
" Inconvertibia paper currency.
1 Present system introduced In 1870, In place of system of 1857 ; 8-gulden piece equivalent to 20 tranca ; silver not freely coined. The Maria Theresa doUat
(■23-0044 grpmrncB, gths fine) ia coined as commercial money.
a The System now in use in tho Scandinaviaa Union (Denmark, Sweden, and Nonv-ay) came into force Ist January 1S76. It Is a monometallic gold etandard
on the decimal system. *
8 The coinage system of Prance came Into /orce 6th May 1709. It was extended to the conntriea composlns the " Latin Union " (Prance, Belgium, Italy,
Switzerland) by the convention of 18t55, and has since been adopted by Greece, Roumania, Scrvin, and Spain. It is thus the most widuly-extended system ft
Kurope. Austria, too, has established some connexion with it by its gold coinage. Tho population using the Latin system has therefore been estimated
Uounial del Ec^nomhtes, April 1879) at 148,000,000. The system Is theoretically a double standard one, with a ratio of 15^ tt> 1 ; but tho statea composing'tho
Union have restricted the coinaRe of silver to a small amount, thus producing what is called tho italon hoUcux, or "limping standard." By it coined silver U
kept above Its market value. The unit In tho different states is called by ditfci-ent names : in Prance, Belgiuu^, and Switzerland, franc and centivw; in Italy,
tlra and cerUetlmo; in Greece, dracfim* and Upta; In Roumania, Ui and bani; In ScrvIa, dfaar and pnru ; in Spain, p«c(a and centesimo; but in all cases tho value
U the same.
' * Tho substitution of the mark for tho older thaJer came Into forcfi Ist J.^nuary 1S7&. The Gennan coinage law is modelled on tho English system, but is
not yet complet«ly settled, owing to ',he largo quantity of Bllvcr in circulation. " '
0 Tlie Dutch standard has been fleveral times change.1. In 1847 a silver standard was adopted, and continued till 1872, the unit being the silver guilder. In
Juno 1875 tho ft-eo coinage of gold was decreed, tho eih-er coinage having been restricted since 1672. Tho ratio of gold to silver Is 15*635 to 1 but practicaUv Iho
>lng standard " c
Tno single gold Btandard Is In force In PortugaL Tho English sovereign is legal tender for 4600 rels.
Tho coins of tho Russian mint are exceptionally gool. They pass as commercial money at varying pric
Finland has a decimal system rescmblin.': U~>4
French since 1877, the mark in gold and siiTer being equivalent to tho franc.
» Tlie Poantnh coinage was assimllat'*d to tho Latin Union In 1S71. Spain, however, coins s SS-pcsota piece; tho other countries of the Union do cot
* The .Mc^JIdlo coinage was Introduced In 1814. English sovereigns circulate at 125 ploslrca, 20-franc piooM at l<iO piast'r^.
MONEY
733
Icrmediate coins are Introdaced, e.g., in Franrc, 2-franc and 5-fxanc
Sieces. In fact, most modem currencies are a combination of the
ecixnal and binary systems, England alone adhering to a motlificd
duodecimal scale. A decimal coinage has for the last sixty yeaia
been proposed for Eiigland, and it is almost certain that if any one
scheme could be pointed out as much preferable to any other it
wouhl be acceptei . As it is, there are two or three proposals, each
commanding some support, while many advocates of the decinia]
system prefer tp wait till an international agreement for its adoption
can be obtained. One of the schemes advanced takes the pi-esent
farthing as' its base ; then 10 farthi-ngs=\ doit (2id.) ; 10 doits— \
f.'jrin (2s, Id.); 10 fiorins=\ pound (208. lOd.). The advantages
of this plan are : (1) that the smaller coins now in use could be
preserved (the penny being 4 farthings), (2) retail prices, which are for
the smaller articles estimated in pence, need not be altered, (3) nor
need those which affect postage, tolls, and mileage charges. Against
^h:5e may be set the loss of the unit of value, the pound, which
should bo raised to 20s. lOd., so that all accounts, and all large
Table III.-
Curreiicies pf th^ mo
c important non- European States.
1
Rem. 1
Approximate ,
Rem. 1
Approximate ]
t
_ . p. 1000. 1
Money Valoj. \
i
_ ^ p. 1000. 1
Money Value. |
Coins.
a
^1
a 1
i
1
1
1
II
SI
Coins.
■3
-c
II
i|
i
•a
11
A. NORTH AMERICA.
States of Colombu?—
e, B. d.
i c
100 Cmtavos 20 Peso piece . .
(}old
32268
900-
S 19 SJ
19 30
British Dominions' —
= 1 Fuo. 10 „
100 Cm(« = l loiter.
(Condor)
16-129
900-
1 19 8
9 65
Mexico!—
is d.
« c
5 Peso piece . .
8-065
900-
0 19 10
4 62
100 Cnii 18 Dollar piece
Gold
27 -067
875-
) 4 9
6 74
2
3-226
900-
0 7 UJ
1 93
= lCoiiar. 8
"
13-5S3
875-
L 12 4)
7 87
* ••
'*
6-767
875-
1 16 2)
3 93
1 „
Silver
25-0
900-
0 8 11}
0 96
s
S-383
875-
0 8 1
1 96
20Centavoa —
,
6-0
836-
0 0 9j
0 19
1
Silver
11192
27-067
675-
900-
0 4 Oi
0 4 0)
0 98
0 93
10
6
;'.
2-5
1-25
836-
836-
0 0 6
0 0 2)
0 10
0 5
60 Cent uiece . .
13-6S3
900-
0 2 0
0 49
25 ;,
6-767
900-
0 10
0 24
Perd'8—
UmTEO St.'TIs»—
imCmltsimot 20 Sol piece....
Gold
32-268
900-
3 19 3{
19 30 ;
100 Cer.ts 20 Dollar pioce
=lSol. 10-
16129
90O-
1 19 8
9 66 1
=1 Dollar. (Double Eagle)
Gold
33-436
900-
2-
1-
4 2 6
6
8-065
900-
0 19 10
4 82 1
10 Dollar piece
2
3-2-25
900-
0 7 11}
1 93 1
(Eagle)
16-718
900-
2-
2-
2 13
1
1-613
900-
0 3 11|
0 96
S Dollar piece
8-S59
5015
900-
2-
2-
1 0 7)
900-
2-
2-
0 12 4j
1 ,
Bflver
25-0
900-
0 8 11
0 96
?' ::
"
4-179
900-
2-
3-
0 10 4
50 Centesimos.
12-5
900-
0 1 11
0 48
"
1-671
900-
2-
8-
0 4 1)
20 „
^^
60
90O-
0 0 9
0 19
10 ,.
'^
2-5
900-
0 0 4:
0 10
1 ..
surer
26-729
900-
3-
5-
0 4 1
6 .,
J.
1-25
900-
0 0 2
0 6
50 Cent piece . .
12-500
900-
3-
6-
0 2 0
25
6-250
900-
3-
6-
0 10
10
2-500
900-
3-
0 0 5
6
1-250
900-
3-
0 0 21
3 ,.
0-802
750-
3-
0 0 l|
C. ASIA.
B. SOUTH AMERICA.
Ahqentink Refoblic ' < —
100 CenUsimos £0 Peso piece . .
= 1 DoUnr lo
(p«o). 5 ;;
Gold
33-S33
900-
4 1 8
19 94
India (British)*—
3Pi«=lPi«. 80 Rnpee piece
4 Piot=l Aita. (DouWe tfohor
OM
23-821
916-4
3 0 0
14 58
;■
16-666
8-335
900-
900-
2 0 10
1 0 5
9 97
4 93
lGAna»=l2tupee. 16 Rupee piece
(Mohur) ...
11-665-
916-6
1 10 0
7 29
*
10 Buoeo piece
7-n2
916-6
1 0 0
4 86
1
SUver
27-11
900-
0 4 1
0 99
5
„
8-8S6
916-6
0 10 0
2 43
Brazil •»—
1
1000 lUis 20 Hilieis piece
Gold
17-927
916'fi
2 4 101
10 91
1
Silver
11-666
916-6
0 2 0
0 43
= lifilT«<. 10
8-963 J916-6
1 S 5*
5 15
••
6 -832
2-916
916-6
916-6
0 1 0
0 0 6
0 24
0 12
2
Silver
25-500 I916-6
0 4 5
1 9
1,
1-458
616-6
0 0 3
0 6
1
18-250
916-6
0 2 2J
0 65
)
6-375
916-6
0 1 1
0 27
Japan* '«-
CniLfe- '
"
100&n=irm. 20Tenpl«e» .
Gold
33-334
900-
4 2 0
19 94
100 Centtpoj 10 Peso piece
= 1 Fuo. (Condor)
10
16-666
900-
2 1 0
9 97
Gold
15-253
900-
1 17 6
9 10
6 tt
8-333
900-
1 0 6
4 98
6 Peso piece . .
2 „
1 „
Silver
7-626
3-051
25-00
900-
900-
900-
0 18 9
0 7 6
0 3 9
4 55
I 82
0 91
2
1
','.
S-S3S
1-tet
900-
900-
0 8 2
D 4 1
1 99
0 99
SO CentsToa piece
20
12-60
5-00
900-
900>
! ! 0 1 101
..(0 0 9
0 45
0 18
50 Sen piece .
20
SUver
10-
1-
800-
800-
0 2 0
0 0 10
0 50
020
10
^^
2-50
900-
..^0 4)
0 9
10
2-
800-
0 0 6
0 10
»
•'<
1-26
900- ..
.. lo 0 2
0 4
5
1-
600-
_11
0 0 2 ' 0 s
• Inconvertible paper currencj. ». , a,- ,
Bemarifcj.— The currencies of such of the non-European States as were capable of being presented fn tabular form have been given above, but a brief outline oi
the crarencies of less-aJvanced countries where a settled coinage does not prevail may be here added. The syst^ma of the various European colonies in America
are, as a rule, similar to their mother-countries. Some of theEnglish possessions acquired by conquest creserve their original currency. In Cayenne tjie pre-
Revolution French money is retained. In Paraguay and Uruguay a much-depreciated paper currency circulates. The Central American states reckon in dollara.
The AuBtralian colonies have a coirency identical with that of England ; the same currency exists in South Africa, In Mauritius the Indian system has been
recently introduced. The various Turkish vassal states possess peculiar coinages. In Egypt, the coins of various European nations form the chief money. The
Asiatic currencies are generally composed of silver. Ceylon has the Indian rnpees. The money of Java has sino* 1 S77 been assimilated to the latest form of the
Dutch monetary system. In China the cash forms the unit, and is made of copper, iron, and tin; silver passes by weight— a tael, which varies from place to
place, being the unit ; whDe the silver jycee is the usual medium of exchange. The other Asiatic currencies do not require particular notice. .v j *
» There ia no currency issued in Canada : English and American coins circuUte. The standard is gold (£1 = 84-60). There were formerly different metIio<IS or
tounting, viz., English sterling, Halifax currency, and Canadian sterling, the respective ratios being 100; 120; IDS.
* The decimal coinage has existed in Mexico since 1867. The gold coins are practically commercial m&ney, nnd command a premium.
» The dollar was introduced in 17S6 as the unit. In 1794 the ratio of gold to silver was fixed at 1 to 15. This valuation underrated gold, consequently siiv«r
became the itta*»dard. In 1834 the ratio was altered to 1 to 16, and it was again changed in 1837. In these changes gold was overrated, and silver was di-iven out
of circulation. This led, in 1853, to the reduction of the metal in the silver coins, which therefore became k token -currency. The suspension of <^sh payments
took place in 1861. Id 1873 silver was demonetized, and gold became the standard. In 1878 the *' Blaud Bill '" was passed, making the silver doUar a le^l
tender, but confining its coinage to the executive, and fixing the amount at from two to four million dollars per month. These silver dollara have not got mco
Jirculation. The UniteiJ States coin a trade dollar of 420 grs. (27-212 grammes), to compete with the Mexican dollar. ^\. in, * ra
* The Argentine Confederation professes to have a gold standanl. The old South American oma weighed 27 grammes, was 876* fine, and worth kn, 43. m
5 The Brazilian system is a depreciated form of *he Portuguese.
« Chili has nominally a double valuation at 1 to I6i\. Gold coins are no longer struck.
' The Colombian States have the Latin Union system, with a ratio of 1 to lb\.
8 When Peru returns to cash payments the system will be almost identical with that of Colombia. * „ , . ,. . ^_ . „
* British India has a single sUver sUndord, as the gold coins are only commercial money. The price of the rupee vanes : gouemUy to recent years it has tmn
* 10 The*old Japaneae couiage consisted of gold cobangs and silver itzibus, with a ratio of I to 4. The system was recast In 18T1, «n(l the PJ^f"^ decimal colnago
adopted, the ratio being I to 1617. The staodard is now practicaUy silver. In 1876 a trade dollar eTactly similar to the Aiaerican trade dollar was iatit>duced.
7:u
M O JN i!J Y
pric« quotations, would have to be altered^ while the new iinit of the
farthing would not be assimilated to any other unit. This plan has
therefore no chance of acceptance. Another proposal starts from
the present pound aa unit. It is to he divided into Idjlorins (23.),
which would contain 100 mila (or farthings reduced 4 per cent.).
A new coin, 10 viils (23. 4d.)i would probably have to be introducecL
The advantages of this plan are : (1) the pound would be preserved
as unit, (2) t\\Qjlorin and shilling would also be retained — the latter
being 60 mils, (3) accounts for large amounts need not be altered.
The objections are such as follow — (1) the copper coins, which
are those most used by the poor, would all be changed, thus causing
great confusion, (2) all charges expressed in pence would be altered
to the loss of one of the parties. Still, this scheme is much to be
preferred to the one first mentioned. A third plan is based on the
fact that 8s. in English money is only |d. more than 10 francs.
Having regard to this link between the English and French systems,
it is proposed to coin a \Q-franG piece in gold to serve as a token
for 8s. If the penny were then reduced by 4 per cent, this piece
would contain 100 pence, and, by coining a franc or tenpenny piece
in silver, a perfect decimal currency would be obtained. This
arrangement would involve the abolition of the pound, as well as of
most of the present English coins. In fact, it is as yet premature
to expect a system which will be international as. well as decimal,
and the most that can be hoped for is some progress towards that
ultimate end. All that can be said at present is that all schemes
for the introduction of the decimal system should be considered with
regard to their tendency to help towards the assimilation of the
English system to other currencies. The problem of international
money has during the last twenty years acquired much prominence.
In previous historic periods the idea was partially realized. Thus
the drachme was an international Hellenic coin, though it had
three different values.^ Under tjie Roman hegemony and the
succeeding empire the denarius became the coin of the west, the
drachme that of the east.^ The next currency which can be called
international was the frequently-mentioned Carlovingian system.
The growth of the different European nationalities, and their frequent
wars, prevented any common coinage system being adopted by tnem.
Each state debased its own coin at different times, so that any
original resemblances disappeared. The question of unification of
the various monetary systems was thus left open for the present
century, when increased facilities for intercourse have led to more
complex inteiTiational relations. An association for promoting unity
in weights, measures, and coins was founded in Paris in 1855, and
actively advocated its principles. In pursuance of this object a
series of conferences and congresses were held on the subject, the
first of them in 1860. The congress of 1863 was held at Berlin, and
adopted a series of important resolutions. Its report advocates the
superior convenience of a gold system with a subsidiary coinage of
silver ; the millesimal scale of 900 as to fineness of the higher coins
was also approved of, as well as the definition of the weights of coins
on the nietnc system. The first practical outcome of the movement
was in the monetary convention of 1865, which founded the so-
called Latin Union, by wliich France, Belgium, Italy, and Switzer-
land became a single monetary region, with the franc or lira as unit.
The subsequent accessions to the Union are given in the note to the
French coinage system (Table II.). In 1867 a monetary conference
was held at trie same time as the Exhibition of that year, when the
idea of a universal coinage was advocated, and three leading principles
were laid down as necessary to that result, viz. — (1) the universal
adoption of a single gold standard, (2) tho general use of the decimal
scale for this coinage, (3) that all coinages should be co-ordinated
with the French system.* Owing to the accidents of historical
development, certain points of connexion existed between the lead-
ing European systems. Thus, the franc being regarded as a unit,
the Austrian florin was as 2*47, the American gold dollar as 5*18,
and the English pound as 25 •22. Very slight changes would bring
these coins into a scries of 1 : 2J : 6 : 25, and it was proposed by the
congress of 1863 that, when thus modified, they should have inter-
national cuVrency in all countries where any of the four units pre-
vailed. All outside nations were recommended to select whichever
of these units tlicy preferred. The subsequent monetary changes
in the various European systems have, however, ended rather in
the formation of inteniational systems without any tendency towards
the establishment of a universal one. Thna, of the three principles
laid down by tlie conference of 1867, two only have been adopted
in recent currency reforms. On the creation of a united Germany
after the Franco-German war of 1870-1871, it was the aim of the
rulers of that country to develop as much as possible all outward
expressions of that unity, and, in accordance with that conception,
a German ciirroncy was devised which was monometallic and decimal
(see Table 11.), but which was not easy to assimilate to the French
system, thus rejecting tho third principle laid dovm by the Paris
conference, and rendering future progress more difficult. The
, Eubolc, and .Eginetan ; seo Sutitb, Diet. Or. aiid Rom. AfU^^ s. v.
Scandinavian Union proceeded on very much the same lines fts th^
German reform, and was, in fact, mainly caused by it. The Dutch
Government, under the pressure of circumstances, have abandoned
the silver standard and coined some gold, but their position is still
undecided. The Austrian Government have made a slight otep by
issuing as gold coins 8- and 4-gulden pieces, which are the same a*
the 20- and 10-franc coins. In one part of the Russian dominions,
Finland, the French system has been introduced, the new mark
being equivalent to the franc. The main Russian system has not
been changed, nor have any alterations been made by England,
Turkey, or Portugal.* The question of universal coinage has
become implicated with the question of the proper standard, and
the strong ground taken up in 1867 has certainly to some extent
been abandoned. It may, nowevcr, be considered that the present
systems of coinage are capable of being assimilated- A comparison
of the amount of pure metal in English, French, German, United
States, and even Japanese coin shows how small is the difference.*
An ingenious proposal was made in 1868 to the English commission
on the question, oy which the sovereign would bo made identical
with the French 25-franc piece (if tliat were coined). It was based
on the fact that tho sovereign contained only about 1 grain more
of gold than the amount in 25 francs. It was proposed to deduct
this small amount from the bullion brought for coinage as seignior-
age, so that no change need be made. The advocates of this scheme
contended that prices would not be affected by the alteration. This
reasoning did not commend itself to the commission. They accepted
the view put forward by Newmarch, who argued that all con-
tracts would have to be altered to allow for the depreciation caused
by the change, and this position seems impregnable, so long as
metallic currency alone is considered. Another mgenious plan was
that of Bagehot to assimilate the English and American systoms, as
a step towards a ^vider change.® At the present moment the great
monetary systems of (1) France and her Edlies, (2) England and the
larger part of.her colonies, and (3) the United States are so firmly
established in their several countries, and the advantages of each
system are" so eoual, that it is hard to see which is to give way.
The wide area of the Latin Union, and the perfect decimal division
of its coinage, are arguments in favour of the franc; the greater
value of the pound, and the immense extent of the English
colonies and English trade, are in favour of the British unit of
value ; while the dollar, from its convenient size and the prospect
of the future growth of the United States, has claims to be con-
feidered in the discussion. The most probable conclusion, however^
seems to be that the future unit will not be any of these coins, but
the result of a compromise, which will lead to a new system being
established. The difficulties which arise when universal coinage
schemes are brought forward ought not to conceal from us the solid
advantages which such an institution would confer on the world-
The arguments urged in its favour ar^ various, and are regarded as
being of different relative importance by their advocates. They
Inay, however, all be stated as follows. (1) Increased facility of
travelling. Though there is a tendency to imder- estimate this
element of tho question, it seems impossible to doubt that the
saving of trouble to travellers by any universal coinage system
would be very great. The abolition even of the local currencies of
Germany and Italy, and their replacement by uniform national
sj'stems, has been a great boon to tourists, but an arrangement
which would obviate the necessity for procuring any different
money whatever would be a still greater advance. In the interests
of peace, which is greatly promoted by extended international
communication, it is very desirable to remove any obstacle which
retards increased intercourse among persons of different countries.
(2) Greater ease in adjusting the foreign exchanges. This argument
has been sometimes pushed too far. It has been appaiently held
that, were a xiniversal currency adopted, the pi-oblems of the foreign
exchanges would no longer exist There are, however, other factora
in the quesHon, namely, those of time and place, which could not be
eliminated by the adoption of a single coinage sj-stcm.' Still, the
removal of even one complicating element wovild simplify exchange
dealings. The quosrion of mint pars would no longer arise, and
the specie points would be stated more simply. The friction wliich
sometimes arises from the necessity of recoining tho exported gold
would also be removed, and tho profits of those dealers who gain by
Aa Austria, Rnssia, and Turkey posscsi fnconvertlble pai^jr currc
variouB foreign coins circulotc In the last-nampd country, the qi;
not posaosB murh importanci
for tliom. Portugal Is closely
1th Engfand. acd will probably follow her exam]>I(
that the gold coins of all these
I 8overoign=7-S2 gma
25 ftnncas=7-20
U. 8. half-c«glc=7-62
Oemian 20 iTwrk=7-16
y also be r
tries have a Queuess of ^Jths.
gold.
tlie flret propOKU nicutlom-d above, but it differs In contemplating the assi
tion of American money, the 5-dollar piece being equivalent to tbe new yc
f See, for this, Qoschcn, Fortign Fxdianges, y. S, and the article Extu
(voL vlii. p. 784 fq). A pimctlcai Illustration is Ibo case of Australia, t^
though the currency la Identical with that of England, bills on England s
« ^remiuDL
MONEY
•35
Hheir special knowledge wonld be saved to ordinary traders. (3)
Tte improvement of the currencies of backward states. Many
countries still possess tiiose mixed currencies whirh were once com-
mon all over Europe, and much confusion consequently arises. The
commercial coins have been introduced for international circulation,*
and a universal currency would perform their function more satis-
factorily. (4) Greater facility in comparing price-lists, kc. This
advantage, which is leserved for the last, has been regarded by
competent judges as the gi'eatest.' It has a practical and a theo-
retical interest : the former, since trade with foreign countries would
' be rendered easier and safer ; the latter, since statistical inquiries
would be very much facilitated. At present, it is quite impossible
for an ordinary trader to understand a set of foreign price-lists, each
perhaps expressed in terms of a different currency from the others, —
a difficulty which is enhanced by the variations of gold and silver
values, not to add the case of an inconvertible paper currency. The
existence of a common monetary langxiage would remove these diffi-
culties, and the premium on gold could be allowed for in the case
of depreciated paper. A much wider development of smaller trading
transactions would become possible, and would add to the world's
wealth. Nor would the greater ease of statistical inquiry be unim-
portant ; the ratjs of wages in different countries, and the profits
on diflerent transactions, would be readily compared, and the move-
ments of labour and capital to the most advantageous points
rendered more rapid. Against these great gains can be set only a
certain and a possible disadvantage — namely, the loss and trouble
involved in change, which would, of course, for the time be con-
siderable, but would soon be over, and the chance that some states
might issue a depreciated currency, which would expel the other
and better coins. In the case of a universal coinage this case would
hardly arise, since there would be no field of employment for the
purer coins, and they would consequently remain in circxilation,
out the whole currency would become depreciated. Proper mint
regulations, however, would obviate this danger, and could surely
bo devised. It may be said that the principal hindrance to one
coinage system for all civilized states is the as yet unsettled ques-
tion of the standard to be employed. Till the debate on this
problem is closed it is vain to expect monetary unification. The
establishment of a universal system based on gold sceir 3d quite
feasible to the conference of 1867, but doubtful to that of 1»78, while
a double standard was the proposal discussed in 1881.
9. Conaideraiions on the Questions arising from the Con-
flict of Standards. — In the preceding section the various
possible monetary systems were set forth, but no discussion
was entered into with respect to their comparative merits.
Only three of these systems need be here examined, namely,
the single standard system, the multiple standard system,
and, lastly, the composite systeln. Nor even is there any
need for examining the various possible single or multiple
standards. The single silver standard is the only one of
the former, as the double gold and silver standard is the
only one of the latter, which need be taken into account.
It is true, historical inquiry has shown that the problem of
the proper proportion between two different metals when
xised together presented itself to the Chinese with regard
to their iron and copper coinages ; but the course of mone-
tary evolution, as discussed in section 3, has resulted in the
rejection of the less valuable metals and in confining the
material of the principal coins to silver and gold. The use
of silver as a principal coinage was, as we have seen, widely
diffused. The Hellenic coins were composed of that metal,
gold being afterwards introduced as a variable commercial
money; and copper was brought in still later as a token
currency. Though copper preceded silver as money in
Kome, the latter, soon after its introduction, succeeded in
displacing it, the ratio firsfr fixed being 1 to 250. A regular
gold coinage did not exist at Eome till the empire, but
gold in bars passed, the legal ratio being 1 to 11-91. StiU
the questions connected with the use of a double standard
do not seem to have arisen.' The various European mon-
archies had silver as their principal money (see p. 726 sg.,
above), gold where it was used being, as in Greece, a
' The principal of these are — the Austrian Jlaria Tlieresa dollar,
the Mcxicau dollar, and the United States UoAe dollar, which is Ti
grs. hervier than the national coin of the same name. See also Table-s
II. and III.
* B.g., Bagehot and Prof. Jevons. The former dwells on the com-
jnercial aspect; the latter noturally places the scientific side first.
' See Mommsen, UUt. of Borne, ii. p. 382 and iv. p. 553.
commercial money. The advance of gold to a position
parallel to silver was commenced in the 13th and continued
in the 14th century, the method of regulating the mixed,
gold and silver currencies being by proclamation, which
fixed the varying ratios from time to time. In England,
this course was followed from the first introduction of
gold coins (1257) to 1663.-' From 1663 to 1717 silver
was the standard, and the gold coins passed at their mar-
ket value. As the silver coins were very much debased,
the gold gtiinea sometimes was deemed equivalent to 303..
After the recoinage of 1696 the guinea passed at 21s. 6d.
At this ratio silver was underrated, and was accordingly
exported to Continental Europe and to India. The loss of
the silver coins aroused the public attention, and the matter
was submitted to Sir I. Newton, whose answer was given
in his Third Representation. He proposed to reduce the-
guinea from 2l3. 6d. to 2I3. as an experimental measure.'*-
The proper reduction for the object in view would have
been to ^Os. 8d. The silver drain, therefore, continued,
and England came to have a gold currency. An opposite
arrangement gave France a silver coinage. The recent
facts of French monetary history, as well as those of the
United States, illustrate the same condition of a-ffairs. The
difficulty of constituting a double standard system on a
secure basis is thus made clear, so far at least as regards a
single country. For the continuance of the two metals in
the currency depends on the market ratio and the legal
ratio between gold and silver being the same. The slightest
examination of the history of these metals will show how
variable they have been. Without accepting the estimates
which regard silver as being more valuable than gold,' the
-well-attested variations of the precious metals have been
very considerable. Thus, Herodotus estimates the ratio a.=i
1 to 13, Plato 1 to 12, Menander 1 to 10, and in Csesar's
time the ratio was 1 to 9.^ Table I. contains the varia-
tions since the discovery of America. In the 14th centuiy'
the value of gold rose remarkably, and the gradual move-
ment has ever since been to-wards an appreciation of gold
relatively to silver. Another point, previously noticed, is
the tendency, as wealth increases, to adopt a more valuable:
form of currency. Gre6ce, Rome, and England all afford,
illustratipns of this movement. The experience of the evils,
of a mixed currency led the earlier -writers on coinage in
England to regard a single standard system as the best, and
silver as the most suitable metal for the standard. Locke,
Petty, and Harris all advocated this view. The earlier
Italian writers proposed to combine gold and silver at a
ratio of 1 to 12, which they conceived to be the actual pro-
portion. The theory of a composite system was, as before
mentioned, first given by Lord Liverpool.' This method
* The various changes made can be estimated from the Tables given;
in James's Essays on Money, &c. ; see also Ency. Brit, 8Lh ed., articles
"Money." A careful statement will be found in Lord Llverpool'K.
work, ch. li.
' Newton's report will be found in Select Tracts on Mo-iiey, edited
by J. E. M'CuUoch for the Political Economy Club (1856). One
passage is worth quoting. " The demand for exportation arises from,
the higher price of silver in other places than in England itn propor-
tion to gold, . . . and may therefore be diminished by lowering th»
value of gold in proportion to silver. If gold in England, or silver in-.
East India, could be brought down so low as to bear the same propor-
tion to one another in both places, there would be here no greater
demand for silver than for gold to be exported to India. And i»' gold
were lowered only so as to have the same proportion to the silver
money in England which it hath to silver in the rest of Europe,
there would be no temptation to export silver rather than gold to any
other pnrl of Europe " (p. 2"; ). The italics are in the original pass-
age, which has beeu much discussed in recent controversies.
' Del Mar, Hist, of the Precious Metals, p. 221. According to
this writer, the variation .has been 200 degrees — t.^., from silver being
10 times as valuable as gold, gold has come to be 20 times more,
valuable than silver.
' Sro Smith, Diet, of Ant., s. v. " Argentom,"
• See above, p. 731.
736'
MONEY
•of regulating the metallic currency was establisned In
En!'l:.iid. as it were, acciJentally, and deliberately adopted
only iu IS 16. The practical good re.sults which loUowed
made all English economists of that period warm advo-
catci of the composite system. Thus, M'CuUoch and
Tooke agree in supporting the English system, as also doea
J. H. Mill.' On the Continent the weight of authority
was more divided, and the existence of the French bi-
metallic system gave support to the advocates of a double
standard. The result of the gold discoveries in Australia
and California was to greatly increase the supply of that
metal, and, under the action of Gresham's law, to change
the French currency from silver to gold, while Holland, to
avoid the evils which were anticipated from the reduced
value of that metal, adopted silver as the standard. The
movements in favour of a universal currency described
above, combined with the course of events, brought the
standard question into greater prominence. The proposal
of the Paris conference of 1867 for a single gold standard,
and a universal coinage on that l-J^ia. raised the question
to great prominence. Wolowski and CourceUe Seneuil
strongly opposed the recommendation, the former predict-
ing that a disastrous appreciation of gold would follow.
This view seems borne out by the result, for, although a
aniversal coinage was not created, yet Gcnnany and the
Scandinavian Union both changed from a eilver to a gold
standard, while Holland and Uie L'nitcd States both made
movements in the same direction by derQcnetizing silver
and making preparations for adopting gold. The Latin
Vnion at the same time restricted their silver coiiiage,wliich
had nearly the same effect as the adoption of a gold stand-
ard.^ TJie result of these extensive changes was to cause
much confusicm. The more ardent advocates of a double
standard, too, attributed most of the continued trade de-
pression to this cause. The altered condition of opinion on
the question was seen at the monetary conference held at
Paris in 1378, where the imiversal demonetization of silver
•was considered to be dangerous. The " Bland Act " of the
United States, which theoretically decreed the double
standard (1878), was another instance of reaction. The
great depreciation of sUvet; which- resulted mainly from its
having ceased to be money over a large part of the civilized
world, severely affected the Indian finances,^ and thus the
advocates of a double standard %vere able to command some
attention in England. The conference held in Paris in
1881 reflected these changed views. The supporters of
the double standard took the initiative and proposed a
treaty based on the double standard at a fixed ratio, but
,no concliLsion was arrived at — England, Germany, and the
Scandinavian Union upholding the gold standard.
Such, in brief, has been the recent liistory of tlie standard question,
and it now becomes desirable to examine moro closely the conflicting
arguments in the various shapes they liave taken. The older English
advocates of the gold standard have found their best representatives
in Lord Liverpool and Tooke. The former of these adopted the
argument used by Petty, Locke, and Harris, that only one metal
can bo the standard of value at a given time, but he held that the
advance of England in wealth rendered gold a mure suitable material
than silver for the principal money. He added that by law the
power lay m the sovereign to settle the standard, and, as a matter
of fact, he contended that gold was actually at that time (1805) Uio
English standard in common estimation. Tlieso arguments were
' ^ Lord Ashburton waa tho only person of influenco who advocata]
the double standard.
* The amounts decreed to bo coined each year were us follows : —
Fn.
1874 = 120,000,000
1875 = 160,000,000
1876 = 120,000,000
1877= 06,000,000
1878= 9,000,0001 t, „ , ,
1879= 20;000;000| F" 't^'y ""ly-
*^ Sco, for a full discussion, "W. Bagehot, Dejtrtciation of SUve. .
supported by a mass of Kistorical examples.* TooVe, who 5eilt ^nrh.
the subject In liia History of Prices^ severely criticizes the double
standard. Ho poiiita out that it would bo impossible to keep hotli
metals in circulation, and that it would bt. the interior one which
would remain. He also indicat'^na moro refined objcv* 'on. uanicly, the
diliiculty of constiturin;j n. uank reserve under the double siandavd-
Thus, if silver were uxa more valuable, and the reserve consisted
mainly of it, there would be an inducement to mako a run on the
reserve, so as to drain out tho small quantity of gold and then get
the more valuable silver." Tho silver standard was preferred hy
Rioardo. who fully arcepted the ar^iments against the double
standard as conclusive ; his view was, that silver was steadier in
value thau Rold, and was the standard money in other countries,
while the objection to it on account of it^ greater bulk w«aa, he
thou^'ht, obviated by tho nw of paper mouey for circulation.* J.
S. ilUl pronounced no opinion as to the comparative merits of gold
and silver, but he objects to the doublo standard on the usual
ground that the cheaper mefal is the only ono used in payments,
and that tlierefore tlie fluctuatious are more frequent under a double
standard regime. The advocates of tlio concurrent use of the two
metals, prominent among whpm were "Wolowski on the Coutiiieflt
and Sevd in England, contended that these objections were ill-
founded, for (1) the double standard, though it produced (t-^.,
admitting the assumption of their opponents) more frequent fluctua-
tions, still did not vary so widely from the mean, since in each case
it was the clicaner metal which determined the value,'' and (2) the
action of Gresham's law would produce a compensatory action.
Tb'is, if silver bo undervalued in a double-standard system, a drain
BotB m ic other countries where it is more valuable. The quantity
of silver ia thus reduced and its value raised, while gold is 'r.j.ortea,
its quantity increased,. &wl. :t3 value lowered. "U'^r^ ^^.u tlie under-
valued metal, tlio converse process would take place. The t-ound-
licss of this position b illustiated by the case of the great transforma-
tion of the French currency (1849-1860). During tlie rapid increase
of the gold supplies the value of silver only rose about 3 per cent. ;
in fact tho depreciation was spread over the two metals, and not
confined to ^old.^ In addition to tho above arguments, it was
urged by "Wolowski that any attempts to establish a universal gold
standaid as contemplated by the Paris conference of 1S67 would
cause a great appreciarion of gold, which would be disastious to
commercial interests, while silver would lose most of it^value. The
services which the double -standard countries rendered by acting as
intermediaries between gold and silver standard countries was also
dwelt on, the ease with which the mass of silver needed for exporta-
tion to the East was supplied from France during the years 1853-56
being an instance in pouit. .The monetary dilficulties, as indicated
above, which followed the adoprion of gold by Gernianv and the
Scandinavian Union, as well as the embarrassment of the Indian
Government, from the resulting depieciaUon of silver, revived tho
double-standard advocates. Cernuschi and De Laveleye cam?
forward as supporters of what the former called Inncfallism, tliat ia
to say, the establishment of a universal, or at all events a large
international, currency, based on the concurrent circulation of the
two metals gold and silver at a fixed ratio. This plau has gained
many supporters, though the tendency among English economists
WHS at first to decline even to consider it ; and not even yet does
tho qucsrion appear to have received that cajeful esamination by
nionoraetallists which would be desirable.^
The bimetallists start with a discussion as to the causes which
determine the value of money. They point out that there are two
extreme theories : ono that the value of money depends ou the wiH
of the sovereign [the fat theory) ; the oilier tliat the value of
money is enrirely independent of state control, and determined by
economic conditions (tnu free trade tJieoryJ. Neither of th&^e is
accepted by the bimetallists. They take up a middle ground and
holtl that, by its power of deciding what substance shall be deemed
legal tender and discharge all obligations, the state is oble to deter-
mine, in'thin liviUs, what substances shall be money and what the
* Coivs of tho Realm, pp. 123-165.
* Thia objection to the double standaid is also srgcd by Prof. Tborold
Rogers and by B-igebot. Actual instances of liiCtlifficulty occurred in
1860, and ngoio in 1876. with the Bank of FYanco.
^ " Proposals for an Economical and Secure Currency,** Works (ed-
M'Culloch), p. 103.
' The superposition of two curves, cvh representing the variations
of one metal, and tlio formation of a third curve reprt.'^enting the
lowest concurrent points of each, will luake this clear. See Jcvons,
MoneUt p. 138.
1 8 See J. E. Caiiues, Essaijs t\i Pot. Koon.^ pp. 140-143.
* Mr A. J. Wilson has collected a seiiea of articles on Rf-iprocity,
Bimetallism, and Land Tenure Reform, and Prof. Bonamv Pfice dealt
with BimetnUi*)m and Fair Trade in his nddrcM to the Social Scleuce
Congress in 1832. But there is no fair reason for plncing fi. de LavrJeye,
Lu7.?ati, Cernuschi. Dana Horton, and other sMpporlers of biraetalhsm
— and we may add Prof. F. A. Walker— in the same cau-gory ^ith tha
advocates of (uo-ralled) "Rociproeily.'*
MONEY
737
▼aim of those saostances shall he. They a?pTL& CronTliifltory that
berera} motals hare hp.on successively deiuonetized, that different
ratios have been- fixed between metals circulating together, that in-
convertible paper currencies have been kept in circulation by the
will of the state.* The docliine of cost of production as determining
the value of money is also assailed by tham. They hold that it is
the quantity of money which governs its value,* and that cost of
production has little or no infiuence in the matter. The next step in
the bimetilKc argument is to contend that their pioposed ratio for
gold to silver (1 to 15^) can be maintained by the legal regulations
to that effect. The common objection to bimetallism is, that which-
ever metal was undervalued would be exported. They Answer that
the same ratio existing over all, or a great part of, the world, there
would be no inducement to export either metal, and in support
of their argument they appeal to the passage from Newton quoted
above, and claim him as the inventor of modem bimetaUism,^
Thirdly, a greater stability as regards v£.lue is claimed for the two
metals combined than for either singly, since the fluctuations are
distributed over a wider field, and, the conditions of production of
gold and silver being somewhat cSfferent, fluctuations in them tend
to counterbalance each other. A fourth point consists in the greater
facilities which would exist for trade, since the fluctuations of the
exchanges which arise from theexistence of gold and silver currencies,
and the variations of relative value of-these metals, would under
-a bimetallic system disappear. The fifth argument for bimetallism
is the advantages which would result from the increased prices
caused by the greater abundance of money, or at all events from
the check to any fall in prices which might arise from a diminution
in the production of gold. The $nal argument is that a universal
currency is desirable, and that, k single gold currency being by
^neral consent practically impossible, this advantageous reform
can be realized in no other way than by adopting a plan which per-
mits the concurrent circulation of two metals. Most of these posi-
tions are contested by the monometallists, and even where any
concession is made the value of the advantage to be reaped Is esti-
mated at a much smaller amount. The contention that the val;:a
of money is largely influenced by state demand is met by the
assertion that cost of production is the ultimate regulator of value,
-and that any artificial regulation would stimulate the production of
the cheaper metal, and thus flood the world with it The fixing of
a ratio dilTerent from the market one is derided by them as absurd,
and an extreme case is instanced for this purpose. la it possible,
they ask, to make the value of silver equal to that of gold ? If not,
how can it be possible to alter the marltet ratio in even the slightest
degree ? Is there not a great demand for the precious mstals in the
\'arious trades ? And would not the ratio of this demand be affected
by the fixing of a new ratio ? The argument of biroetallists that
their system would produce greater stability in the value of money
is met by the answer that there is no proof of this. It is quite
possible that a single metal may be steadier in value than two com-
bined, and the evidence of history shows that silver is more liable
to depreciation than gold. The argument derived from the advan-
tages to exchange transactions is to a slight extent admitted, but
it is pointed out that the factors which affect the foreign exchanges
are so numerous, and are so rapidly eliminated in the course of
trade, that a radical currency change need not be adopted for this
purpose. It is also shown that, even when most European countries
were bimetallic, fluctuations in the exchange price of silver took
place ; and stiH more that, where it is the less valuable metal that
IS in course of depreciation, bimetallism can afford no aid. The
assumed tendency of the bimetallic scheme to produce a higher
scale of prices than would otherwise prevail is dwelt on by oppo-
nents as a proof of its inherently vicious character. The claim to
benefit the world by adding to its stock of money places himetal-
tists in the same class with the advocates of inconvertible paper
money, and shows the absence of reason in their views. Their
position becomes the same as that of the Birmingham currency
schooL The proposition that the quantity of money is of no con-
sequence since prices vary in proportion to it is cited as conclusive,
and the contempt so frequently expressed for bimetallists is ac-
counted for by their advocacy of this principle of the beneficial
effects of an increased amount of money. To the contention that
bimetallism is the necessary condition for a universal coinage system
the answer is, that the idea of universal coinage is premature, and
that the gradual introduction of the gold standard is desirable as
preparing the way for a future universal coinage based on gold
monometallism. On the practical question as to the actual intro-
duction of the system, the monometallists deny the possibility of
1 See Daua Horton's paper on the Position of Law in the Doctrin4 qf Money,
presented to the monetary conference of 18S1 (Appendix ix C).
* On p, 721, above, the theory of money value has been stated, and the objec-
tions to the cost of prodcction theory given. It is strange to find Jevons
arguing (in common with Bagehot and Prof. Price) that the value of money
ultimately depends on cost of production, when his examination of that doc-
trine in general is conaidered. Compare ConUmp, Rev. (May 18S1) with Jevons's
Thwry of Pol Eeon., p. 201 »q.
* Hodem blmetalUslB freely admit that two different bimetallic systems—
I.e., :!-ring different xatloB— could not e:ast, for each would drain the oUter of
forming a unffcreSI RareSUlTleagire which Would not he liable to
be broken up by war, or impaired by some of the states which com-
' pos^d it issuing inconvertible paper. On the otiier hajid, the various
international conventions for postal pui-poses, extradition, com-
mercial arrangements, and other matters of interest, are considered
by bimetallists as evidences of the feasibility of their plan.*
The above summary gives the main arguments on each side
of the discus^on as given by the advocates of the contending
principles. A short consideration will show that the controversy
may be suitably divided into three heads, viz. — (1) the possibility
of constructing a universal bimetallic system which shall be in
accordance with sound economic principle ; (2), if the first question
be answered in the affirmativi, the comparative merits of this
system as opposed to the present variety of systems, or a futiu'e
universal gold-standard system : and (3) the expediency undcfr
present circumstances of nations m general, and England in parti-
cular, joining in the proposed convention. Each of these topics
calls for some remai-k. (1) The possibility of a bimetallic system
can hardly be denied. Under all the difficulties attending its
existence in a single countiy, it was retained in practical work-
ing in France during the early part of the 18th century, and it
is plain that a widely-extended league would afford a better field
for its action. It is quite possible that national preferences for one
metal '-" the other would be displayed, but this would be no
hindrance, since the exchanges would be related by the legal rate,
and prices would depend on the total quantity of both metals
(the amount of gold being multiplied by the legal ratio, and added
to the amoiint of silver).*^ The objection which denies the power of
Governments to fix the relative values of gold and silver, and which
is supported by the instance of the extreme case of silver being
made equal in value to gold, may be set aside by the consideration
that the use of the precious metals takes two forms — (a) their use
as commodities, (b) their use as money. Since the state can
influence the demand for these metals as money, and since therefore
it can raise the value of either of them by this increased demand, it
follows that, within assignable limits, it can fix the ratios between
them, and that these limits are *'the i-atio which would subsist
between their values if gold were demonetized, and that which
would subsist if silver were demonetized."* The possibility of bi-
metallism, if oil nations were agreed, is allowed by some mono-
metallists {e.g^, Professor Je\Gcs}, and an unconscious argument to
this effect was given by the proposal of Chevalier, at the time of the
Australian gold discoveries, to adopt silver as the standard and
demonetize gold, which is a clear recognition of the force of law in
monetary questions. It is therefore reasonable to answer in che
bimetallists' favour the question fiist raised. (2) The corsiderations
to be taken into account under the second head are far more com-
plex, and do not admit of accurate determination. The present
currency systems of England and "the Scandinavian Union are
based on the composite system, and afi"ord the greatest satisfaction
to the inhabitants of those countries. The bimetallic system of
the Latin Union has been suspended, the introduction of silver
as the principal money not being desired by the various peoples
concerned. Germany has lost considerably by the sales of depre-
ciated silver, and, were a gold standard once firmly established, it
is not lilcelythat any wish for change would be manifested. "With
silver countries the case is different. They have to receive masses
of depreciated silver and to give commodities in exchange, while
their purchasing power is reduced owing to the greater relative
value of gold to silver. It would therefore be clearly advantageous
for silver-using countries that a system should be adopted which
would raise the value of their money, and save them from the
necessity of importing large quantities of silver to produce a proper
adjustment. The ultimate consequences of the complete demone-
tization of silver as regards silver- using countries are not so clear.
The supply of gold might suffice for all wants, and might furnish
abetter currency than the 'heavier silver. The preservation of
two separate monometallic systems, of gold for the more advanced
countries of Europe and the United States, of silver for Russia and
India, would, when the superfluous stock of silver had "passed to
the East, present little difficulty after equilibrium' was attained.
The new ratio between silver and gold would become established,
and silver prices in silver-using countries would he higher in pro-
portion to the fall in the value of silver. It is therefore plain that
a suitable adjustment would be reached under any variety of
currency systems, and it may therefore be concluded that the
comparative merits of the competing standards are not capable of
* The principal sources for the above summary, besides works before cited,
are the pamphlets of 8eyd, Cemuschi, and De lAveleye, on the bimetallist
side, as well as the articles of the latter in the Fort, and CoiUemp. Revirw$.
The m6nometalli8t arguments are given by Prof. Jevons (ConUmp., May 1881X
Mr R. Giffen (Essays in Financt, pp. 286-310), and Lord ^erbrooke (Nineteenth
Century, April 1882). See also the Bepoi-t of the Paris conference, 1881, and
Mr T. H. Farrer, The StaU in Us Selation to Trade^ pp. 49 52.
s It is assumed that the other Eactora which Influence the value cX money
(see p. 722, above) remain constant.
6 Mr J. J. Mnrphy in Dublin StcxHstical JoumaJ., vol viU. p. 282. Bee also
M. Walras, Journal (Ut Bconomiitcs, May ISSl, "Tli^orie Uath6mati%u9 da
bimdtalhame."
XVL — 93
738
M 0 N — M 0 N
bein^ decided "at present. The immediate introduction of a
universal /^old currency ia by the admisision of all parties eminently
undesirable, and this is the only settled point ia the controversy.
(3) Tlie iast head which the bimetallic question embraces is the
practical e.\i>cdiency of joining in a bimetallic league with
1 ratio of 1 to 15^. "With "regard to this aspect of the question
tho answer, for England at least, ought to bo a negative one. The
present Engli^h monetary system has worked well. It is iirnjy
rooted in English habits, and is not therefore to be lightly aban-
doned. Again, the intcresta of English creditors are plainly opposed
to any movement calculated to raise the value of silver relatively to
gold, and to depreciate prices in general. Tho threat of some bi-
metallists, that all nations will bo driven to adopt a gold standard,
and thus produce a crisis in tho English money market by the
resulting gold drain, is of no weight ; any drain of English gold will
hav« to be paid for at a high price, and tho simple expedient of
raising the uank-rato will restore as much bullion as is needed in
England. Tho interests of other countries cannot be so clearly
determined. A state like Germany, holding a largo stoi'o of depre-
ciated silver, may desire other states to become bimetallic, but will
hardly desire to do so herself. Tho interests of India and other
silver-standard countries have been considered before. When all
these aspects of the question have been examined the most probable
conclusion is, that the chances of a bimetallic league in the imme-
diate future are very small, and that future monetary evolution will
be ruled rather by the course of events, and the pressure of circum-
stances in each separate state, than by the ccmscious deliberations
of an international conference.
Bibliogrnphy. — The literature of the vai-ious questions connected
with money is very extensive, and only a brief notice of it can be
given here. The principal authority among the Greeks is Aristotle,
who in two passages {Kic, Efk., v. 5 ; Pol., i. 9} has discussed the
qualities of money, and pointed out its functions with great clear-
ness. Xenophon also, in his work Oti the Athenian Utate, dealt
with the value of the precious metals, though his views are partially
erroneous. The only passages worth noticing in Latin literature
are those of Pliny, who seems to have held a form of th» mercantile
theory, and Paulus, who, in a fragment preserved in the Digest, has
treated of the origin of money. The mediaeval literature embraces
several works dealing specially with the question of changes in the
standard of money, which were condemned by the theologians. The
first treatise professedly on the special subject of money is a work
by Nicholas Oresme, bishop of Lisieux (o6. 1382), entitled De Originc,
Natura, Jure, ct Mutationibu^ Monetarum, reprinted in 1864 (Paris)
by Wolowski, and even now worth reading. The next work to
be noticed is the De Monctantm Potcstatc simul ct Utilitatc libellus
(Nuremberg, 1542), a fragment of a larger treatise on economics, of
Gabriel Biel {ob. 1495). It has been remarked that "the favourite
Subject of the economists of the 16th century was that of money."
The first of these works to be noticed is De Monets CudcndsR Paiione
by Copernicus, reprinted along with the work of Oresme above
mentioned. At a later date the Jesuit Mariana discussed the varia-
tions in prices under the title Dc Mvnetx Afutationc. In the same
century an anonymous work appeared in German, with the title
Gemein^ Stiinm€nA>on dcr Muntzc (1530). In 1588 Davanzati issued
Lesione delle Monete, advocating a bimetallic system. The problem
of the elevation of prices caused by the American mines led to the
issue of several works, owe of tho most remarkable being the
Dialogues of William Staflbrd (1581).
In the 17th century Sir W. Petty dealt with money in a tract.
Quantulumcnmgue (1682). The recoinage of 1696 called fortli-
Lowndes's Esaay for the Amendment of the Silver Coins, and Locke't
Further Cwisiderations conecmiiig raising thi Value of Money. In
the 18th century the Tfcjwrte of Sir I. Newton, as Master of the Mint,,
are valuable. Cantillon's Essai (Paris, 1755) contains in its 2d and
3d parts a sound account of currency. Harris's £ssay on Money '
and Coins (1757) is also useful. An earlier tract by Rice Vaughan,
Discourse of Coin and Cuinage (1675), is brief, but correct in prin-
ciple. Adam Smith's Ip'calth of Kations (London, 1776) discusses
the subject of money ia B. i. chs. 4 and 5, while seigniorage is
examined in B. iv. ch. 6. The treati.sc. The Coins of tht Rcolm
(London, 1805), by tho first earl of Liverpool, elaborately disrasscd
the question of tho proper standard, and has powerfully influenced
monetary legislation in England and Germany. Ricardo'i pam-
lihlets on the bullion question added to the knowledge of the laws
which regulated a depreciated currency. Senior, in his I^edures
on the Cost of obtaining Money (London, 1829), developed the theory
of the international distribution of the precious metals.
The last half century has been a time of active discussion regard-
ing monetary questions, — the gold discoveries, international coin-
age, decimal coinage, bimetallism, the resumption of specie pay-
ments in countries where an inconvertible currency has existed,'
each of these topics having had its special literature. Some of these
works have been mentioned when dealing with the special questions
they refer to, and these, in turn, refer to nisny others. It will
suffice here to mention more general works. The theory of money
is dealt with by the leading English economists in their systematic
works (ilill. Principles, B. iii. chs. 7-10, 19, 21 ; Fawcett, Manual,
B. iii. chs. 5, 6, 15, 16 ; Shadwell, System, B. iiL chs. 1-3 and 8),
also by Cherbuliez (Pricis, B. ii. ch. 3, vol. i. and B. iL ch. 3, vol.
ii.). Chevalier has devoted the third volume of his Cours (Paris,
1842-50) to the subject, with the title of " La Monnaie." The late
Professor W. S. Jevons's valuable work. Money and the Mechanism of
Exchange, and Professor Hussey Walsh's concise Treatise on Metallic
Currency (Dublin, 1850) may also be useji. More elaborate than
either of these is F. A. Walker's Money, the most comprehensive,
work on the sufjject in English ; his smaller work. Money in its
Relation to Trade and Industry, is likewise very good. Wolowski's
VOr et V Argent contains much information, as does also Knies's
Das Geld. E. Seyd's Bullion and Foreign Exchanges is serviceable,
but the changes since its publication (1869) deprive it of most of
its value. The various editions of Tate's Cambist give the most
accurate (though often imperfect) statements as to the facts of
currency. Jacob's work on The ■ Producticn and Consumption of
the Precious Metals gives many interesting details, though the
conclusions are often fanciful, and the authorities relied on not
trustworthy. The recent work of Del Mar, History of the Precious
Metals (London, 1880), furnishes a criticism and continuation of
Jacob, and supplies many new details. His criticism of the
" cost \J production " theory as applied to gold and silver is especi-
ally useful. Some of his views on the moral aspects of the question
need qualification. Professor Sumner's History of the American
Currency may be relied upon for its facts. The Reports of the various
conferences also supply abundant information on their special topics.
Among those may be mentioned the Proceedings of the Paris con-
ferences of 1867, 1878, and 1881 ; the Decimal Coinage Commission
(1868) ; the French Enqutk Monitaire (1870) ; and the Report of the
Committee of the House of Commons on the Depreciation of Silver
(1876). The Reports of the (English) Mint furnish information as to
the coinage changes of each preceding year. (C. F. B, ^
MONFERRATO, or Montferrat, an ancient marquisato
of North Italy, in the valley of the Tanaro, the name of
which still survives in the luUer title (Casale Monferrato)
of the town of Casale. The princes of Monferrato were
among the most powerful Italian families of the Middle
Ages. Among them were several famous crusaders :
Conrad, prince of Tyre from 1187 to 1192, the valiant
opponent of Saladin ; and Boniface, king of The.ssalonica
from 118.3 to 1207. In 1303, on the extinction of the
male line, the marquiaate passed to Theodore Pala;ologU3
through his mother, the empress Irene. The Palajologi
became extinct in 1533. The duchy was subsequently
attached to Mantua, and ultimately absorbed in Savoy in
the beginning of last century.
MONQE, O.ispARD (1746-1818), French mathemati-
cian, the inventor of dcscri[)tive geometry, was born at
BcT.une on the 10th May 1740. He was educated first at
the collc;];c of the Oratorians at Beaune, and then in their
college at Lyons, — where, at sixteen, the year after he had
been learning physics, he was made a teacher of it.
Returning to Beaune for a vacation, he made, on a large
scale, a plan of the town, inventing the methods of obser-
vation and constructing the necessary instruments ; the
plan was presented to the town, and preserved in their
library. An officer of engineers seeing it WTOte to recom-
mend Mongo to the commandant of the military school at
Miziires, and he was received as draftsman and pupil in
tlio practical school attached to that institution ; the
school itself was of too aristocratic a character to allow of
his admission to it. His manual skill was duly appreci-
ated : "I was a thousand times tempted," he said long
afterwards, "to tear up my drawings in disgust at the
esteem in which they were held, as if I had been good for
nothing better." An opportunity, however, ]ircscnted itself:
being required to work out from data supplied to him tho
" defilement " of a proposed fortress (an operation then
only performed by a long arithmetical process),'* Monge,
substitutine for this a geometrical method, obtained the
M O N— M O N
739^
result 80 quickly that the commandant at first refused to
receive it — the time necessary for the work had not been
taken ; but upon examination the value of the diocovery
was recognized, and the method was adopted. And llonge,
continuing his researches, arrived at that general method
of the application of geometry to the arts of construc-
tion which is now called descriptive geometry. But such
was the system in France before the Revolution that the
officers instructed in the method were strictly forbidden
to communicate it even to those engaged in other branches
of the public service; and it was not until many years after-
wards that an account of it was published. The method
consists, as is well known, in the use of the two halves of
a sheet of paper to represent say the planes of xy and xz
at right angles to each other, and the consequent repre-
sentation of points, lines, and figures in space by means
of their plan and elevation, placed in a determinate relative
position.
In 1768 Monge became professor of mathematics, and
In 1771 professor of physics, at M^ziires; ia 1778 he
married Madame Horbon, a young widow whom he had
previously defended in a very spirited manner from an
unfounded charge; in 1780 he was appointed to a chair
of hydraulics at the Lyceum in Paris (held by him together
with'his appointments at Meziferes), and was received as k
member of the Academy ; his intimate friendship with
Bertliollet began at this time. In 1783, quitting Meziferes,
he was, on the death of Bezout, appointed examiner of
naval candidates. Although pressed by the minister to
prepare for them a complete course of mathematics, he
declined to do so, on the ground that it would deprive
Madame Bezout of her only income, arising from the sale
of the works of her late husband ; he wrote, however
(1786), his Traite ilementaire de la Statique.
Monge contributed (1770-1790) to the Memoirs of the
Academy of Turin, the Memoires des SavanU JEtrangers of
the Academy of Paris, the Memoires of the same Academy,
and the Annates de Chimie, various mathematical and
physical papers. Among these may be noticed the memoir
" Sur la th^orie des d6blais et des remblais " (Mem, de
i'Acad. de Parts, 1781), which, while giving a remarkably
elegant investigation in regard to the problem of earth-
work referred to in the title, establishes in connexion with
it his capital discovery of the curves of curvature of a
surface. Euler, in his paper on curvature in the Berlin
Me/noirs tot 1760, had considered, not the normals of the
surface, but the normals of the plane sections through a
particular normal, so that the question of the intersection
of successive normals of the surface had never presented
itself to him. Monge's memoir just referred to gives the
ordinary differential equation of the curves of curvature,
and establishes the general theory in a very satisfactory
manner ; but the application to the interesting particular
case of the ellipsoid was first made by him in a later paper
in 1795. A memoir in the volume for 1783 relates to
the production of water by the combustion of hydrogen ;
but Monge's results in this matter had been anticipated
by Watts and Cavendish.
In 1792, on the creation by the Legislative Assembly
of an executive council, Monge accepted the office of
minister of the marine, but retained it only until April
1793. "When the Committee of Public Safety made an
appeal to the savants to assist in producing the materiel
required for the defence of the republic, he applied him-
self wholly fo these operations, and distinguished himself
by his indefatigable activity therein ; he wrote at this
time his Description de I'art defabriquer les canons, and
his Avis axuc ouvriers en fer tvr la fabrication de I'acier.
He* took a very active part in the measures for the
establishment of the Normal School (which existed only
during the first four months of Jie year 1795), and of
the School for Public Works, afterwards the Polytechnic
School, and was at each of them professor for descriptive-
geometry ; his methods in that science were first pub- ■
lished in the form in which the shorthand writers took,
down his lessons given at the Normal School in 1795, and'
again in 1798-99. In 1796 Monge was sent into Italy
with Berthollet and some artists to receive the pictures
and statues levied from several Italian towns, and made
there the acquaintance of General Bonaparte. Two years
afterwards he was sent to Bome on a political mission,
which terminated in the establishment, under Massena, of
the shortlived Roman republic ; and he thence joined the
expedition to Egypt, taking part with his friend Berthollet,
as well in various operations of the war as in the scientific
labours of the Egyptian Institute of Sciences and Arts ;
they accompanied Bonaparte to Syria, and returned with
him in 1798 to France. Monge was appointed president
of the Egyptian commission, and he resumed his connexiou
with the ?„lyteclmic School. His later mathematical
papers are published (1794-1816) in the Journal and the
Correspondance of the Polytechnic School. On the forma-
tion of the Senate he was appointed a member of that:
body, with an ample provision and the title of count of
Pelusium ; but on the fall of Napoleon he was deprived of
all his honours, and even excluded from the list of mem-
bers of the reconstituted Institute. He died at Paris on
the 28th July 1818.
For further information see B. Brisson, Notice hisiariqxie sut
Gaspard Monge ; Dupin, Easai historique rur la services et la tra-
vatix scicntijiqua de Gaspard Monge, Paris, 1819, which contains,
(pp. 162-166) a list of ilonge's memoirs and works ; and the bio-
graphy by Arago {(Euvra, t ii., 1854).
Alonge's various mathematical papers are to a considerable
extent reproduced in the Applkalion de FAnalyse d la Giamitrie,
4th edition (last revised by the author), Paris, 1819 — the pure text
of this is reproduced in the 5th edition (rev-ue, coi-rigee et annotaa
par M. Liouviile), Paris, 1850, which contains also Gauss's Jlcmoir,
" Disquisitiones geneiales circa superficies curvas," and some vain--
able notes by the editor. The other principal separate works are
Traite ilementaire de la Statique, 8' edition, canformie A la prici-
dtnte, par M. Bachette, et suivit oCitne Note etc, par M. Cauchy,
Paris, 1846; and the Oiomitrie Descriptive (originating, as mentioned,
above, in the lessons given at the Normal School). 'The 4th edition,
published shortly after the author's death, seems to have been sub-
stantially the same as the 7th [Giomiirie Descriptive par G. Monge,
suivie (Tune thiorie da Ombra et de la Perspective, extraite dapapiers
de I'aiUeur, par M. Brisson, Paris, 1847). (A. CA.)
MONGHTR, or MnifGrR, a district in the lieutenant-
governorship of Bengal, lying between 24° 22' and 25° 49'
N. lat., and 85° 40' and 86° 52' R long., is bounded on
the N. by Darbhangah and Bhigalpur, on the E. by Bh&gal-
pur, on the S. by the SantAl Parganis and HazAribdgh, and
on the W. by Gay4, Patni, and Darbhangah, with an area
of 3922 square miles. The Ganges divides the district
into two portions. The northern, intersected by the Burl
Gandak and TiljugA, two important tributaries of the
(ranges, is always liable to inundation during the rainy
season, and is a rich, flat, wheat and rice country, support-
ing a large population. A considerable area, immedi-
ately bordering the banks of the great rivets, is devoted to
permanent pasture. Immense quantities of buffaloes are
sent every hot season to graze on these marshy prairies ;
and the ghi, or clarified butter, made from their milk
forms an important article of export to Calcutta. 'i< To the.
south of the Ganges the country is dry, much less fertile,
and broken up by fragmentary ridges. The soil consists
of quartz, mixed in varying proportions with mica. Ranges
of hills intersect this part of the district, and in the
extreme south form conical peaks, densely covered with
jungle, but of no great height. Irrigation is necessary
throughout the section lying on the south of the Ganges.
In 1872 the population of MonghjT was 1,812,986 (malen
897,074 : females 91£,912): Hindus, 1,613,S4S ; Uobammedanal
740
M O N — M O N
182,269 ; the remainder, consisting mainly of aboriginal tribes and
bill races, profess primi' cj forma of faith. There are alsd a few
Buddhists and Christiantj. Seven towns contained upwards of
5000 inhabitants in 1872— Monghyr, 59,698 ; Shaikhpura, 11,530 ;
Jamalpur, 10,453; Barbiy^, 10,406; Surijgarha, 7935 ; Barbigha,
13362 ; and Jamiii, 5197. No trustworthy statistics of the area under
cultivation exist since the revenue survey in 1847, when it was
returned at 1,311,768 acres ; it is known, however, that cultiva-
tion has largely extended since then. The land is held principally
onder the tenure known as bkdoli-jot, by which the tenant pays
rent, either in money or in kind, according to the out-turn of his
crops in each year. It is of ancient standing, and popular with
the tenantry. Monghyr is famous for its manufactures of iron :
firearms, swords, and iron articles of every kind are produced in
Abundance, but are noted for cheapness rather than quality. The
irt of inlaying sword-hilts and other articles with gold and silver
affords employment to a few families. The most important manu-
facture, however, is that of indigo, conducted by means of Euror
pean capital and under European supervision. The total area
under indigo is estimated at about 10,000 acres, with an average
out-turn of 2900 cwts. of dye. Minor industries include weaving,
dyeing, cabinet-making, boot-making, soap-boilino;, and pottery.
The principal exports, sent to Calcutta both by rail and river, are
oil-seeds, wheat, rice, indigo, gram and pulse, hides, and tobacco ;
and the chief imports consist of European piece goods, salt, and
sugar. , The valueof the formerin 1876-77 was £430,000, andofthe
latter £314,000. Education is making f;iir progress, and in 1^74-
76 there were 229 Government and aided schools, attended by 6675
pupils. The climate is dry and healthy. The temperature is high
in the hot weather, reaching 107* Fahr. in May ; bat the cold
weather is cool and pleasant. The 5vcrag9 ann-ual rainfall is 46J
inches. Malarial fever is comparatively uncommon, but epidemics
of cholem occur frequently.
Monghyr was one of the principal centres of the Mohammedan
administration in Bengal. In the early years of Brilish rule,
Itonghyr formed a part of Bhagalpur, and was not created a
separate district till 1832.
MoNGHYE, chief town ana administrative headquarters
of the above district, is situated on the south bank of the
Ganges (25° 22' N. lat., 86" 30' E, long.). The population
in 1872 was 59,698: viz., Hindus, 44,900; Mohammedans,
14,346; Buddhists, 33; Christians, 305; "others," 24.
In 1195 Monghyr, a fortress of great natural strength, appears to
have been taken by Muhammad Bakhtyar Khilji, the first Aloslem
conqueror of Bengal. Henceforth it is often mentioned by the
Mohammedan chroniclers as a place of military importance, and
was frequently chosen as the seat of the local government. After
1590, when Akbar established his supremacy over the Afghan
chiefs of Bengal, Monghyr was long the headquarters of his general,
Todar Mall ; and it also figures prominently during the rebellion
of Sultan Shuja against his brother, Aurangzeb. In more recent
times Nawab Mir Kasim, in his war with the English, selected it
as his residence and the centre of his military preparations. The
fame of Monghyr armourers is said to date from the arsenal which
he established. The town is now purely a civil station, and in
some respects one of the most picturesque in Bengal.
MONGOLS
THF early history of the Mongols, like that of all
central-Asian tribes, is extremely obscure. Even the
meaning of the name " Mongol " is a disputed point, though
a genera! consent is now given to Schott's etymology of the
frord from " mong," meaning brave. From the earliest
and very scanty notice we have of the Mongols in the
history of the T'ang dynasty of China (a.d. 619-90) and
in works of later times, it appears that their original
camping-grounds were along the courses of the Kerulon,
Upper Nonni, and Argun rivers. But in the absence of
all historical particulars of their origin, legend, as is usual,
has been busy with their early years. The Mongol historian
Ssanang Ssetzen gives currency to the myth that they sprang
from a blue wolf ; and the soberest story on record is that
their ancestor Budantsar was miraculously conceived of a
Mongol widow. By craft and violence Budantsar gained
the chieftainship over a tribe living in the neighbourhood
of his mother's tent, and thus left a heritage to his son.
Varying fortunes attended the descendants of Budantsar,
but on the whole their power gradually increased, until
Tesukai, the father of Jenghiz Khan, who was eighth in
descent from Budantsar, made his authority felt over a
considerable area. How this dominion was extended under
the rule of Jenghiz Khan has already been shown (see
Jenghiz Khan), and when that great conqueror was laid
to rest in the valley of Keleen in 1227 he left to his sons
en emoire which stretched from the China Sea to the banks
t>l tne Dnieper.
Over the whole of this vast region Jenghiz Khan set his
Second surviving son Oghotai or Ogdai as khakan, or chief
khan, while to the family of his deceased eldest son Juchi
he assigned the country from Kayalik and Kharezm to
the borders of Bulgar and Saksin " where'er the hoofs of
Mongol horses had tramped ; " to Jagatai, his eldest sur-
viving son, the territory from the borders of the Uigur
country to Bokhara ; while Tuld, the youngest, received
charge of the homo country of the Mongols, the care of the
imperial encampment and family, and of the archives of
the state. The ajipointment of Ogdai as his successor, be-
ing contrary to the usual Mongol custom of primogeniture,
gave rise to some bitterness of feeling among the followers
of Jagatai. But the commands of Jenghiz Khan subdued
these murmurs, and Ogdai was finally led to the throne
by his dispossessed brother amid the plaudits of the
assembled Mongols. The ceremony was completed by
Ogdai making three solemn genuflexions to the sun, and
by the princes taking an oath by which they swore " that
so long as there remained of his posterity a morsel of fi«ah
which thrown upon the grass would prevent the cows from
eating, or which put in the fat would prevent the dogs
from taking it, they would not place on the throne a prince
of any other branch." In accordance with Mongol customs,
Ogdai signalized his accession to the throne by distribut-
ing among his grandees presents from his father's treasures,
and to his father's spirit he sacrificed forty maidens and
numerous horses. Once fairly on the throne, he set himself
vigorously to foUow up the conquests won by his father.
At the head of a large army he marched southwards into
China to complete the ruin of the Kin dynasty, which had
already been so rudely shaken, while at the same time Tule
advanced into the province of Honan from the side of Shense.
Against this combined attack the Kin troops made a vigor-
ous stand, but the skill and courage of the Mongols boro
down every opposition, and over a hecatomb of slaughtered
foes they captured Kai-fung Foo, tie capital of their ene-
mies. From Kai-fung Foo the emperor fled to Joo-ning
Foo, whither the Jlongols quickly followed. After sus-
taining a siege for some weeks, and enduring all the horrors
of starvation, the garrison submitted to the Mongols, and
at the same time the emperor committed suicide by hang-
ing. Thus fell in 1234 the Kin or "Golden" dynasty,
which had ruled over the northern portion of China for
more than a century.
But though Ogdai's first care was to extend his empire
in the rich and fertile provinces of China, he was not
forgetful of the obligation under which Jenghiz Khan's
COTiquests in western Asia had laid him to maintain his
supremacy over the kingdom of Kharezm. This was the
more incumbent on him since JelAl al-din, who had been
driven by Jenghiz into India, had returned, reinforced by
the support of the sultan of Delhi, whose daughter he had
married, and, having reconquered his hereditary domains,
had advanced westward as far as Tiflis and Khelat. Once
more to dispossess the young sultan, Ogdai sent a force
of 300,000 men into Kharezm. With such amazing i«-
pidit}- did this army march in pursuit of its foe that the
MONGOLS
741
advanced Mongol guards reached Amid (Diarbelir), wkilher
JelAl al-din had retreated, before that unfortunate sovereign
had any idea of their'' approach. Accompanied by a few
follcvers, Jeldl al-dln fled to the Kurdish mountains, where
he was basely murdered by a peasant. The primary object
of the Mongol invasion was thus accomplished; but, with
the instinct of their race, they made this conquest but a
Btepping-stona to another, and Avithout a moment's delay
pushed on still farther westward. Unchecked and almost
unopposed, they overran the districts of Diarbekr, Meso-
potamia, Erbll; and Khelat, and then advanced upon
Azerbijan. So great was the terror with which these
fierce warriors inspired the people of the provinces they
attacked that single Mongols are said to have slain tlie
inhabitants of entire villages without a hand having been
raised against them. In the following year (1236) they
invaded Georgia and Great Armenia, committing frightful
atrocities, sparing neither man nor woman, young nor old,
with the exception of those whom they saved to ipinister
to their wants or passions. Tiflis was among the cities
captured by assault, and Kars was surrendered at their
approach in the vain hope that submission would 'gain
clemency from the victors. Meanwhile, in 1235, Ogdai,
whose troops were as numerous as their thirst for conquest
was devouring, despatched three armies in as many direc-
tions. One was directed against Corea, one against the
Sung dynasty, which ruled over the provinces of China
80Uth of the Yang-tsze Keang, and the third was sent west-
ward into eastern Europe. This last force was commanded
by Batu, the son of Juchi, Ogdai's deceased eldest brother,
who took with him the celebrated Sabutai Bahidur as his
chief adviser. Bulgar, the capital city of the Bulgats, fell
before the force under Sabutai, while Batu pushed on over
the Volga. With irresistible vigour and astonishing speed
the Mongols made their way through the forests of Penza
and Tamboff, and appeared before the " beautiful city " of
Riazan. For five days they discharged a ceaseless storm
of shot from their balistas, and, having made a breach in
the defences, carried the city by assault on the 21st of
December 1237, "The prince, ^-ith his mother, wife,
sons, the boyars, and the inhabitants, mthout regard to
^e or sex, were slaughtered with the savage cruelty of
Mongol revenge ; some were impaled, some shot at with
arrows for sport, others were flayed or had nails or splinters
of wood driven under their nails. Priests were roasted
alive, and nuns and maidens ravished in the churches
before their relatives. 'No eye remained open to weep
for the dead.'" Moscow, at this time a place of little
importance, next fell into the hands of the invaders, who
then advanced against Vladimir. After having held out
for several days against the Mongol attacks, the city at
length succumbed, and the horrors of Riazan were repeated.
The imperial family, with a vast crowd of fugitives, sought
shelter in the cathedral, only to perish by the swords of the
conquerors or by the flames which reduced it to ashes. If
possible, a more dire fate overtook the inhabitants of
Kozelsk, near Kaluga, where, in revenge for a partial
defeat inflicted on a Mongol force, the followers of Batu
held so terrible a " carnival of death " that the city was
renamed by its captors Mobalig, " the city of woe." With
the tide of victory thus strong in their favour the Mongols
advanced against Kieff, "the mother of cities," and carried
it by assault. The inevitable massacre followed, and the
city was razed to the ground. While the scene of blood-
ehed was at its height a catastrophe occurred which at
any other time would have been considered of supreme
horror. Under the weight of a vast crowd of fugitives
the flat roof of the metropolitan church fell in, burying
dl, young and old, in a vast hecatomb.
Victoriouc and always advancing, the Mongols, havin"
desolated this portion of Russia, moved on in two divisions,
one under Batu into Hungary, and the other under Baidar
and Kaidu into Poland. Without a check, Batu marched
to the neighbourhood of Pesth, where the whole force o£
the kingdom was arrayed to resist him. The Himgarian
army was posted on the wide heath of Mohi, which is
bounded by "the vine-clad hills of Tokay," the mountains
of Lomnitz, and the woods of Diosgyor. To an army thus
hemmed in on all sides defeat meant nlin, and Batu
instantly recognized the dangerous position in which his
enemies had placed themselves. To add to his chances of
success he determined to deliver his attack by night, smd
while the careless Hungarians were sleeping he launched
his battalions into their midst. Panic-stricken and help
less, they fled in all directions, followed by their merciless
foes. Two archbishops, three bishops, and many of the
nobility were among the slain, and the roads for two days'
journey from the field of battle were strewn with corpses.
The king, ""la IV., was saved by the fleetness of his
horse, though closely pursued by a body of Mongols, who
followed at his heels as far as the coast of the Adriatic,
burning and destroying everything in their way. Mean-
while Batu captured Pesth, and on Christmas Day 1241
having crossed the Danube on the ice, took Gran by assault
While Batu had been thus triumphing, the force under
Baidar and Kaidu had carried fire and sword into Poland.
At their approach the inhabitants of Cracow deserted the
city, after having given it over to the flames. Disappointed
at the loss of their expected spoil, the Mongols advanced
to Wahlstatt in the neighbourhood of Licgnitz, where the
Polish army under Duke Henry 11. of Silesia awaited their
onslaught. With savage impetuosity, the troops of Baidar
rushed to the attack, and completely defeated the Poles.
As usual, no quarter was given. The massacre was fright-
ful, and Duke Henry himself was amongst the slain. It
was a Mongol habit to cut off an ear from each corpse ol
their slaughtered f oes> and on this occasion it is said thr '
they filled nine sacks with these ghastly trophies. Follow
ing the example of the inhabitants of Cracow, the peopl.
of Liegnitz left but the blackened walls of what had onc(
been the town as a prey for the Mongols, who without
delay pushed south-eastward into Moravia as far as the
vicinity of Troppau. AVhile lajnng waste the country in
the neighbourhood of that town, they received the an-
nouncement of the death of Ogdai, and at the same time
a summons for Batu to return eastwards into Mongolia.
While his lieutenants had .been thus carrying his arms
in all directions, Ogdai had been giving himself up to
ignoble ease and licentiousness. Like many Mongols, he
was much given to drink, and it was to a disease produced
by this cause that he finally succumbed on the 11th of
December 1241. He was succeeded by his son Kuyuk, who
reigned only seven years. Little of his character is known,
but it is noticeable that his two ministers to whom he left
the entire conduct of aSairs were Christians, as also were hi>
doctors, and that a Christian chapel stood before his tent.
This leaning towards Christianity, however, brought no
peaceful tendencies with it. On the contrary, we hear of
an advance against the sultan of Rum (Asia Minor), and of
an expedition into Syria, by which that country was made
tributary to the Great Mongol empire, of a fresh campaign
against Corea, and of another attack on the Sung dynasty
of China. On the death of Kuyuk dissensions which had
been for a long time smouldering between the houses of
Ogdai and Jagatai broke out into open war, and after
the short and disputed reigns of Kaidu and Chapai, grand-
sons of Ogdai, the lordship passed away from the hoiise
of Ogdai for ever.
On the 1st of July 1251 Mangu, the eldest son of jrarg-.,
Tul^, and nephew to Ogdai, was elected khakan. With Kban,
742
ai
0 .^1 G O L y
l>erfect imijai-tiaiit), Maiigu alluwed the light of hia coun-
tenauce to fall upon the Christians, Mohammedans, and
Buddhi.^ta among his subjects, although Shamanism was
.recognized &.t tliu »tat« religion. Two years after his
.accession his court was visited by Rubruquis and other
Chii.'stian monks, who were hospitably received. The de-
scription given by Rubiuquis of the khakan's palace at
Karakorum shows how wide was the interval which sepa-
i-atcd him from the nomad, tent-living life of his fore-
iatheis. It was ".surrounded by brick walls. . . . Ita
southern side had three doors. Its central hall was like a
cJiuich, and consisted of a nave and two aisles, separated
■ hy columns. Here the court sat on great occasions. In
front of the throne was placed a silver tree, having at its
base foui lions, from whose mouths there spouted into
four silvei basins >vine, kumiss, hydromel, and terasine.
At the top of the tree a silver angel sounded a trumpet
when the reservoirs that supplied the four fountains wanted
leplenisliing." On his accession complaints reached Mangu
tliat dissensions had broken out in the province of Persia,
and he therefore sent a force under the command of his
'ffolngu. orothei Hulagu to punish the Ismailites or Assassins, who
were held to, be the cause of the disorder. Marching
by Samarkand and Kesh, Hulagu crossed the Oxus and
advanced by way of Balkh into the province of Kohistan.
The terroi of the Mongol uame induced Rokn al-din, the
chief of the Assassins, to deprecate the WTath of Hulagu
ty offers of submission, and he was so far successful that
he was able to purchase a temiMrary immunity from mas-
sacre by dismantling fiftj of the principal fortresses in
Kohistan. But when once the country had thus been left
at the mercy of the invaders, their belief in the old saying
" Stone dead hath no fellow " sharpened thfeir battle-axes,
and, sparing neither man, woman, nor child, they extermin-
ated the unhappy people. Hulagu then marched across
the snowy mountains in the direction of Baghdad. On
arri^ ing before the town he demanded its surrender. This
being lefused, he laid siege to ihe walls in the usual destruc-
tive Mongol fasliion, and at length, finding resistance hope-
less, tlie caliph was induced to give himself up and to open
the gates to his enemies. On the 15th of February 1263
the Mongols entered the walls, and, following their in-
stincts, sacked the city. For seven days it waa given up
to pillage, fire, and the sword, and the number of killed
Tvas said to have reached the enormous sum of 800,000.
For the moment the caliph's life was spared, and he was
allowed to carry away 100 wives out of 700 who lived in
liis harem, as being those upon whom " neither the sun
nor moon had shone." But his fate soon overtook him.
Accounts differ as to the circumstances of his death, some
saying that he was sewn up in a sack and trodden to
<leath by horses, others that he was starved to death. To
the Moslem world his lo.s3 was a religious catastrophe, as
by it Islam lost its spiritual head. While at Baghdad
Hulagu gave his astronomer, N^dsir al-dln, permission to
Ijuild an observatory. The town of ilaragha was the site
chosen, and, under the superintendence of Nisir al-din and
iour western Asiatic astronomers who were associated with
iim, a handsome observatory was built, and furnished with
*' armillary spheres and astrolabes, and with a beautifully-
executed terrestrial globe sho^ving the five climates." One
terrible result of the Mongol invasion was a fearful famine,
■which desolated the provinces of Irak-Arabi, Mesopotamia,
Syria, and B)lm. But, though the inhabitants starved, the
Jlongols had strength and ener;jy left to continue their
onward march into Syria. Aleppo was stormed and
sacked, Damascus surrendered, and Hulagu was meditating
the capture of Jerusalem with the object of restoring it to
the Christians when he received the news of Mangu's death,
and, as ia dutv bound, at once set out on his return to
Mongolia, leaving Kitubuka in command of the Mongol
forces in Syria. As a reward for his services, HuJagu
received the investiture of his conquests, and established
there the empire of the likhans.
While Hulagu was prosecuting these conquests in western
Asia, Mangu and his ne.\t btcther Kublai were pursuing
a like course in southern China. Southward they even
advanced into Tong-king, and westward they carried their
arms over the frontier into Tibet. But in one respect there
was a vast difference between the two campaigns. Under
the wise command of Kublai all indiscriminate massacres
were forbidden, and probably for the first time in Mongol
history the inhabitants and garrisons of captured cities
were treated with humanity. While carrying on the war
in the province of Sze-ch'uen Mangu was seized with an
attack of dysenter}', which proved fatal after a few days'
illness. His body was carried into Mongolia on the backs
of two asses, and, in pursuance of the custom of slaughter-
ing every one encountered on the way, 20,000 persons
were, according to Marco Polo, put to the sword.
At the Kuriltai, or assembly of notables, which was held
at Shang-tu after the death of Mangu, his brother Ku-
blai (see KtTELAi Khaji) was elected khakan. For
thirty-five years he sat on the Mongol throne, and at his
death in 1294, in his seventy-ninth year, he was succeeded
by his son Timur Khan, or, as he was otherwise called,
Uldsheitu Khan. The reign of this sovereign was chiefly
remarkable for the healing of the division which had for
thirty years separated the families of Ogdai and Jagatai
from that of the ruling khakan. Uldsheitu was succeeded
by his nephew Khaissan. In accordance with the usual
ceremony, on the election being announced four of the
princes of the blood raised the new khakan aloft on a
piece of white felt, two others supported him, while a
seventh offered him the cup. " Meanwhile, while Shaman
offered up prayers for his prosperity and sahitcd him by
the title of Kuluk Khan, carts full of gold pieces and rich
tissues were brought out and distributed. So many pearls
were spread on the ground that it resembled the sky.
The feast lasted a week, during each day of which 40 oxeij
and 4000 sheep were consumed. libations of milk froia
700 sacred cows and 7000 ewes were sprinkled on the
ground." With that tolerance which so markedly char-
acterized the Mongols at this period, Kuluk worshipped
indiscriminately at the temples of the Chinese Shang-te
and before the Buddhist shrines, while at the same time
he lent a favourable countenance to John of Montecorvino,
who, during the whole of his reign, was archbishop of
Peking. Unfortunately the archbishop was not so tolerant
as the khakan, and carried on as fierce a dispute ^ith the
Nestorlan Cnristians of his day as that which divided the
Dominicans and Jesuits in China three centuries jater.
After a sWjrt reign, and at the early age of thirty-one, Kuluk
was gathered to his fathers in February 1311. His nephew
and successor, Buyantu, was a man of considerable culture,
and substantially patronized Chinese literature. Among
other benefits which he conferred on letters, he rescued
the celebrated inscription -bearing "stone drums," which
are commonly said to bo of the Chow period (B.C. 1122-
2.'5.5), from thu decay and ruin to which tuey were left by
the la.st emperor of the Kin d) nasty, and placed them in
the gateway of the temple of Confucius at Peking, where
they now stand. After a reign of nine years Buyantu was
succeeded by his son Gegen, who perished in 1323 by the
knife of an assassin, — the first occasion on which a reigning
descendant of Jengliiz Khan thus met his fate. Yissun
Timur, who was the next sovereign, devoted himself mainly
to the administration of his empire. He di\'ided China,
which until that time had been apportioned into twelve
piovinces, into eighteen provinces, and rearranged th«
MONGOLS
743
■systea of state granaries, which had fallen into disorder.
His court was visited by Friar Odoric, who gives a minute
description of the palace and its inhabitants. Speaking
of the palace this writer says —
" Its basement was raised about two paces from the ground, and
within there were twenty-four columns of gold, and all the walls
were hung with sKns of red leather, said to be the finest In the
world. In the midst of the palace was a great jar more than two
paces in height, made of a certain precious stone called merdacas
(jade) ; its nrice exceeded the value of four large towns. . . . Into
this vessel clrink was conducted by certain conduits from the court
of the palace, and beside it were many golden goblets, from which
those drank who listed. . . . When the khakan sat on his throne,
the queen was on his left hand, and a step lower two others of his
women, while at the bottom of the steps stood the other ladies of
luS family. All those who were married wore upon their heads the
foot of a man as it were a cubit and a half in length, and at the
top of the foot there were certain cranes' feathers, the whole foot
being set with great pearls, so that if there were in the whole world
any fine and large pearls they were to be found in the decoration
of those ladies *'
The following years were years of great natural and
political convulsions. Devastating floods swept over China,
carry iog death and ruin to thousands cf homes ; earthquakes
made desolate whole districts ; and in more than one part
of the empire the banners of revolt were unfurled. The
khakans who now successively occupied the throne, instead
of striving to stem the tide of discontent and disorder, gave
themselves up to every kind of debauchery. As a natural
consequence, the conduct of afiairs fell entirely into the
hands of their ministers, who but too often reflected fhe
vices of their sovereigns. A comet which appeared in the
Toghon reign of Toghon Timur Khan, and which was believed to
Timor be the precursor of fresh disaster^, to the reigning house,
•Xhan. justified the prediction by being almost immediately fol-
lowed by an earthquake, which overthrew the temple of
the Imperial Ancestors, from the altars of which, as if to
complete the misfortune, the silver tablets of the emperors
were in the consequent confusion stolen. It was not long
before the popular discontent found vent. In order to
prevent the recurrence of the periodical inundations caused
by the overflow of the Yellow river, the emperor ordered
a levy of 70,000 men to excavate a new channel for its
dangerous stream, and imposed a heavy tax ^ meet the
necessary expenses. These oppressive edicts overstrained
the patience of the people, and they broke into open re-
bellion. Under various leaders the rebels captured a num-
ber of cities in the provinces of Keang-nan and Honan,
and took possession of Hang-chow, the capital of the Sung
emperors. At the same tinae pirates ravaged tho coasts
and swept the imperial vessels off the sea. While
these combined disorders were disturbing the coimtry, the
emperor, under the guidance of Tibetan Lamas, was being
initiated into the sensual enjoyments peculiar to the warmer
climates of Asia.
In 1355 a Buddhist priest named Choo Tuen-chang
became so impressed with the misery of his countrymen
that he threw off his vestments and enrolled himself in
the rebel army. His military genius soon raised him to
the position of a leader, and with extraordinary success
he overcame With his rude levies the trained legions of
the Mongol emperor. While unable to defeat or check
the rebels in the central provinces Toghon Timur was also
called upon to face a rebellion in Corea. Nor were his
arms more fortunate in the north than in the south. An
army which was sent to suppress the revolt was cut to
pieces almost to a man. These events made a dream
which the emperor dreamt about this time of easy inter-
pretation. He saw in his sleep " a wild boar with iron
tusks rush into the city and wound the people, who were
driven hither and thither without finding shelter. Mean-
while the sun and the moon rushed together and perished."
'*11u8 dream," said the diviner, "is a prophecy that the
khakan will lose his empire." The fulfilment followed
closely on the prophecy. By a subterfuge, the rebels, after
having gained possession of most of the central provinces
of the empire, captured Peking. But Toghon Timur by
a hasty flight escaped from his enpmies, and sought safety
on the shores of the Dolonor in Mongolia. For a time the
western provinces of China continued to hold out against
the rebels, but with the flight of Toghon Timur the Mon-
gol troops lost heart, and in 1368 the ex-Buddhist priest
ascended the throne as the first sovereign of the Ming or
" Bright " dynasty, under the title of Hung- woo.
Thus ended the sovereignty of the house of Jenghiz
Khan in China, nor need we look far to find the cause of
its fall Brave and hardy the Mongols have always shown
themselves to be ; but the capacity for consoUdating tho
fruits of victory, for establishing a settled form of govern-
ment, and for gaining the allegiance of the conquered
peoples, have invariably been wanting in them. For a
time their prowess and the exceptional ability of some of
the first emperors of their line held the people of China
in a bondage which was only outwardly peaceful, and,
when the hands which held the reins lost their nervous
power, and the troops, enervated by the softer climate of
China, lost much of their hardihood, the long pent-up
hatred of a foreign yoke broke out and with gathering
strength drove the invaders back to their Mongolian
pasture-ground.
Not content with having recovered China, the emperor
Hung-woo sent an army of 400,000 men into Mongolia in
pursuit of the forces which yet remained to the khakan.
Even on their own ground the disheartened Mongols
failed in their resistance to the Chinese, and at all points
suffered disaster. Meanwhile Toghon Timur, who did
not long survive his defeat, was succeeded, in tho
khakanate by Biliktu Khan, who again in 1379 was
followed by Ussakhal Khan. During the reign of this last
prince the Chinese again invaded Mongolia, and inflicted
a crushing defeat on the khan's forces in the neighbour-
hood of Lake Buyur. Besides the slain, 2994 officers and
77,000 soldiers are said to have been taken prisoners, and
an immense booty to have been secured. This defeat
was the final ruin of the eastern branch of the Mongols,
who from this time surrendered the supremacy to the
western division of the tribe. At first the Keraits or
Torgod, as in the early days before Jenghiz Khan rose
to power, exercised lordship over the eastern Mongols,
but from these before long the supremacy passed to the
Oirad, who for fifty years treated them as vassals. Not-
withstanding their subjection, however, the Keraits still
preserved the imperial line, and khakan after khakan
assumed the nominal sovereignty of the tribe, while the
real power rested with the descendants of Toghon, tho
Oirad chief, who had originally attached them to his
sceptre. Gradually, however, the Mongol tribes broke
away from all governing centres, and established scattered
communities with as many chiefs over the whole of
eastern Mongolia. The discredit of having finally disin-
tegrated the tribe is generally attached to Lingdan Khan
(1604-1634), of whom, in reference to his arrogant and
brutal character, has been quoted the Mongolian proverb :
"A raging khakan disturbs the state, and a raging
saghan (elephant) overthrows his keepers."
At this time the Mongob, though scattered and in The
isolated bodies, had recovered somewhat from the shock ^^
of the disaster which they suffered at the hand of the first
Ming sovereign of China. When first driven northwarcU,
they betook themselves to the banks of the Kerulon, from
whence they had originally started on their victorious
career; but gradually, as the Chinese power became weake)
among the frontier tribes, they again pushed southward?
744
MONO 0«L S
and at this time had established colonies in the Ordus
country, within the northern bend of the Yellow river.
The Mongol royal family and their immediate surroundings
riconpied the Chakhar country to the north-v/est of the
Ordus territory, where they became eventually subjugated
by the Manchus on the overthrow of the Ming dynasty
in 1614 by the present rulers of China. Possibly out of
consideration for the royal descent of their chiefs, the
Chinese emperors have invariably placed these Mongols
in a privileged position, and have incorporated the eight
banners or military divisions of the Chakhars as one of
the eight banners of the' imperial Manchu army. The
remaining Mongols who submitted to the Manchus were
divided into 135 banners, 49 representing all those on
the south-east of the desert, and 86 the Khalkhas, whose
territory stretched along the north of the desert from
the neighbourhood of Barkhul on the west to the Dalai-
nor on the north-east. From and before this period the
liistory of the eastern Mongols has been that of all the
nomad tribes of central Asia, about which nothing can
be more certainly said than that that which appears most
improbable is most likely to happen, and that that which
might naturally be expected rarely, occurs. Each tribe,
as its fortunes varied, either rose to power or sank into
insignificance. At times the old vigour and strength
which had nerved the arm of Jenghiz Khan seemed to
return to the tribe, and we read of successful expeditions
being made by the Ordu Mongols into Tibet, and even of
invasions into China. The relations with Tibet thus
inaugurated brought about a rapid spread of Buddhism
among the Mongolians, and in the beginning of the 17th
century the honour of having a Dalai Lama born among
them was vouchsafed to them. In 1625 Toba, one of the
sons of Bushuktu Jinung Khon, went on a pilgrimage to
the Dalai Lama, and brought back with him a copy of the
Tanjur to be translated into Mongolian, as the Kanjur
had already been. But though the prowess of the Ordu
Mongols was still unsubdued, their mode of living was as
barren and rugged as the steppes and rocky hilLs which
make up their territory. Their flocks and herds, on which
they are entirely dependent for food and clothing, are not
numerous, and, like their masters, are neither weU fed nor
well favoured. But though living in this miserable condi-
tion their princes yet keep up a certain amount of barbaric
state, and the people have at least the reputation of being
honest. Several of the tribes who had originally migrated
■with those who finally settled in the Ordu territory, finding
the country to be so inhospitable, moved farther eastward
into richer pastures. Among these were the Tumeds, one
of whose chiefs, Altan Khan, is famous in later Mongol his-
tory for the power he acquired. For many years during the
16th century he carried on a not altogether unsuccessful
Vr-ar with China, and filially, when peace was made (1571),
the Chinese were fain to create him a prince of the empire
and to confer a golden seal of authority upon him. In
Tibet his arms were as successful as in China ; but, as has
often happened in history, the physical conquerors became
the mental subjects of the conquered. Lamaism has
always had a great attraction in the eyes of the Mongols,
and, through the instrumentality of some Lamaist prisoners
whom Altan brought- back in his train, the religion spread
at this time rapidly among the Tump,fL;. Altan himself
embraced the faith, and received at his court the Bogda
Sodnam Gyamtso Khutuktu, on whom he lavished every
token of honour. One immediate effect of th.e introduction
of Buddhism among the Tumeds was to put an end to the
sacrifices which were commonly made at the grave of their
chieftains. In 1584 Altan died, and was succeeded by his
son Senge Dugureng Timur. The rich territory occupied
by the Tumeds, together with the increaaed iatercourae with
China which sprang up after the wars of Altan, began to
effect a change in the manner of life of the people. By
degrees the pastoral habits of the inhabitants became more
agricidtural, and at the present day, as in Manchuria, Chinese
immigi-ants have so stamped their^ mark on the fields and
markets, on the towns and villages, that the country has
become to all intents and purposes part of China proper.
Passing now from the inner division of the Mongols — that . iio
is to say, the Chakhars and the 49 banners who Live in the '^''''1
southern and eastern portions of the desert — we come to the " '^'
outer division, which is divided into 86 banners, ana
occupies the territory to the north of the desert. Cf these
the chief are the Khalkhas, who are divided into the West-
ern and Eastern Khalkhas. These people form the link of
communication between Eui'ope and easteru Asia. Early
in the 17th century the Russians sent an embassy to the
courtof the Golden Khan with the object of persuading the
Mongol khan to acknowledge allegiance to the czar. This
he did without much hesitation or inquir}', and he fur-
ther despatched envoys to Moscow on the return of the
Russian embassy. But the allegiance thus lightly acknow-
ledged was Ughtly thrown off, and in a quarrel which broke
out between the Khirghiz and the Russians the Khalkhas
took the side of the former. The breach, however, was
soon healed over, and'we find the Golden Khan sending
an envoy again to Moscow, asking on behalf of his master
for presents of jewels, arms, a telescope, a clock, and "a
monk who had been to Jerusalem that he might teach the
Khalkhas how the Christians prayed." Their submission
to Russia on the north did not save them, however, from
the Chinese attacks on the south. In central Asia, as
the recent history of Russia in that part of the world
shows, the depredations of a tribe on the property of its
neighbours supply a ready cause of quarrel at any moment,
and the Chinese had no difficulty, therefore, in justifying
an invasion of the Khalkha territory. At that time the
present Manchu dynasty ruled in China, and to the then
reigning sovereign the Khalkhas gave in their submission.
For some time the Chinese yoke sat lightly on their
consciences, but difficulties having arisen with the Kal-
muks, they were ready enough to claim the protection of
China. To cement the alliance the emperor K'ang-he
invited all the Khalkha chiefs to meet him at the plain
of Dolonor. This ceremony brought the separate history
of the Khalkhas to a close, since from that time they have
been engulfed in the Chinese empire.
Another important branch of the great Mongolian family^
is the tribe of the Koshod or Eleuths. These claim that
their chieftains have maintained unbroken the direct descent
from Khassar, a brother of Jenghiz Khan. Their home
is in the neighbourhood of the Koko-nor, and in the country
to the north of the narrow strip of the Kansuh province
which separates that district from Mongolia proper. The
pasture in the territories thus indicated is rich and abund-
ant, and the Eleuths have therefore had fewer temptations
to wander than most of their cognate tribes. Being thus
stationary and within a short distance of the Chinese fron-
tier, they easily fell under the dominion of that empire, and
in the year 1725 were incorporated into 29 imperial banners.
During the Kin dyfla^ty of China the Keraits, as has
been pointed out, were for a time supreme in Mongolia,
and it was during that period that one of the earliest
recognized so^■ereign3, Merghus Buyuruk Khan, sat on the
throne. In an engagement with a neighbouring Tatar
tribe their khan was captured and sent as a propitia-
tory present to the Kin emperor, who put him to death
by nailing him on a wooden ass. On the treacherous
Tatar chief the widow determined to avenge herself, and
chose the occasion of a feast as a fitting opportmilty.
With well-disguised friendship she sent him a present ot
MONGOLS
745
tea oxen, a hundred sheep, and a hundred sacks of kumiss.
Hiese last, however, intitaid of being filled with skins of
the liquor which Mongolians love so well, contained armed
men, who, when the Tatar was feasted, rushed from their
concealment and killed him. A grandson of Merghus was
the celebrated Wang Khan, who was sometimes the ally and
sometimes the enemy of Jenghiz Khan, and has also been
identified as the Prester John of early Western writers. La
war he was almost invariably unfortunate, and it was with no
great difficulty, therefore, that his brother Ki Wang detached
the greater part of the Kerait tribes from his banner, and
The founded the Torgod chieftainship, named probably from
'Xotgod. jjjg country where they settled themselves. The unrest
peculiar to the dwellers in the Mongolian desert, disturbed
the Torgod as much as their neighbours. Their history
for several centuries consists of nothing but a succession
of wars with the tribes on either side of them, and it was
not until 1672, when Ayuka Khan opened relations with
the Russians, that the country obtained an even temporarily
settled existence. Its position, indeed, at this time made
it necessary that Ayuka should ally himssH either vrith the
Russians or with his southern neig'- hours the Turks, though
at the same time it was obvious that his alliance with the
one would bring bim into coUision with the other. His
northern neighbours, the Cossacks of the Yaifc and the
Bashkirs, both subject to Russia, had the not uncommon
propensity for invading his borders and harassing his sub-
ject3. This gave rise to complaints of the czar's govern-
ment and a disposition to open friendly relations with the
Blrim khan. A rupture with Russia followed, and Ayuka
carried his arms as far as Kasan, burning and laying waste
the villages and towns on his route and carrying off prisoners
and spoils. Satisfied with this vengeance, he advanced no
farther, but made a peace with the Russians, which was
confirmed in 1722 at an audience which Peter the Great
gave him at Astrakhan. On Ayuka's death shortly after
this event, he was succeeded by his son Cheren Donduk,
who received from the Dalai Lama a patent to the throne.
But this spiritual support availed hun little against the
plots of his nephew Donduk (^mljo, who so completely
gained the sufftages of the people that Cheren Donduk
fled before him to St Petersburg, where he died, leaving
his nephew in possession. With consummate impartiality
tue Russians, when they found that Donduk Ombo had
not only seized the throne but was governing the country
with vigour and wisdom, formally invested him with the
khanate. At his death he was succeeded by Donduk
Taishi, who; we are told, went to Moscow to attend the
coronation of the empress Elizabeth, and to swear fealty
to the Russians. After a short reign he died, and his
throne was occupied by his son Ubasha. The position of
the Torgod at this time, hemmed in as they were between
the Russians and Turks, was rapidly becoming unbearable,
and the question of migrating " bag and baggage " was
very generaUy mooted. In the war between his two power-
ful neighbours in 1769 and 1770, Ubasha gave valuable
assistance to the Russians. His troops todk part in the
siege of Otchakoff, and gained a decided victory on the
Kalans. Flushed with these successes, he was in no mood to
listen patiently to the taunts of the governor of Astrakhan,
who likened him to a "bear fastened to a chain," and he
made up his mind to break away once and for all from a
tutelage which was as galling as it was oppressive. He
determined, therefore, to migrate eastward with his people,
and on the 5th of January 1771 he began his march with
70,000 families. In vain the Russians attempted to recall
the fugitives, who, in spite of infinite hardships, after a
journey of eight months reached the province of Ili, where
they were welcomed by the Chinese authorities. Food
for a year's consumption was supplied to each family;
and khd, money, and cattle were freely distributed. How
many lost their lives on the toilsome march it is impo*
sible to say, but it is believed that 300,000 persons sur-
vived to receive the hospitality of the Chinese. This
migration i» interesting as illustrating the many displace-
ments of triLjs and peoples which have taken place on
the continent of Asia at different periods of history. Such
another migration occurred between four and five thousand
years ago, when the Chinese crossed from western Asia
into their present empire ; such, again, was the movement
which carried ' the Osmanli Turks from north-eastern Asia
into Asia Minor, and eventually across the Bosphorus.
By this desperate venture the Torgod escaped, it is true,
the oppression of the Russians, but they fell into the hands
of other masters, who, if not so exacting, were equally de-
termined to be supreme. The Chinese, flattered by the
compliment implied by the transference of allegiance,
settledthem on lands in the province of Li, in the neigh-
bourhood of the Altai Mountains, and to the west of the
desert of GoM. But the price they were made to pay for
this liberality was absorption in the Chinese empire. Like
the other Chinese -subdued Mongols, the Torgod were
divided into banners, and from that time forth they lost
their individuality.
Among the Mongol chiefs who rose to fame during the
rule of the Ming dynasty of China was Toghon, the Kal-
muk khan, who, taking advantage of the state of confusion
which reigned among the tribes of Mongolia, established
for himself an empire in north-western Asia. Death carried
him off in 1444, and his throne devolved upon his son
Ye-seen, who was no degenerate offspring. Being without
individual foes in Mongolia for the same reason that
Narvaez had no enemies — namely, that he had killed them
all — ^he turned his arms against China, which through all
■history has been the happy hunting-ground of the northern
tribes, and had the unexampled good fortune to t.ke
prisoner the Chinese emperor Ching-tung. But victory
did not always decide in his favour, afid, after having .■suf-
fered reverses at the hands of the Chinese, he deemed it
wise to open negotiations for the restoration of h'" itaperial
prisoner. Tlius, after a captivity of seven years, Ching-
tung re-entered his capital in 1457, not altogether to the
general satisfaction of his subjects. On the death of Te-seen,
shortly after this event, the Kahnuks lost much of theis
power in eastern Asia, but 1-etained enough in other por-
tions of their territory to annoy the Russians by raids
within the Russian fror.rier, and by constant acts oT pillage>
In the 17th century their authority was partly restored by
Galdan, a Lama, who succeeded by the usual combination G/.idab
of wile and violence to the throne of his brother SenghiS. Khnn,
Having been partly educated at Lhasa, he was well versed
in Asiatic politics, and, taking advantage of a quarrel be-
tween the Black and White Mountaineers of Kashgar, he
overran Little Bokhara, and left a viceroy to rule over the
province with his capital at Yarkand. At the same tin: ^
he opened relations with China, and exchanged presents
with the emperor. Having thus secured his powerful
southern neighbour, as he thought, he turned his arms
against the KhaUdias, whose chief ground of offence was
their attachment to the cause of his brothers. But his rest-
less ambition created alarm at Peking, and the emperor
K'ang-he determined -to protect the Khalkhas against *heir
enemy. Great preparations were made for the campaign.
The emperor, in person commanding one of the two forces^
marched into Mongolia. After enduring incredible hard-
ships during the march through the' desert of Gobi the im-
perial army encountered the Kahnuks at Chao-modo. Th,6
engagement was fiiercely contested, but ended in the con^
plete victory of the Chinese, who pursued the Kahnuks fof
10 miles, and completely dispersed their force.'. Immense
746
MONGOLS
numliers were slain, among whom was Gaidan's wife, and
many thousands surrendered themselves to the victors.
Oaldan, with his son, daughter, and a few followers, fled
westward and escaped ; and thus collapsed a power which
had threatened at one time to overshadow the whole of Cen-
tral Asia. For a time Galdan stiU maintained a semblance
of resistance to his powerful enemy, and death overtook
him while yet in the field against the Chinese. The news
of his death was received with great rejoicings at Peking.
The emperor held a special service of thanksgiving to Heaven
for the deUverance vouchsafed, and ordered that the ashes
of his enemy, whose body had been bm-ned, should be
brought to the capital and there scattered to the four
winds. The fear which had been thus inspired was no idle
terror. Galdan was a man to be feared. The conqueror
of Samarkand, Bokhara, Urgenj, Kashgar, Hami, and
twelve hundred other towns, might well be considered a
formidable foe, and Heaven a merciful deliverer in ridding
Asia of so restless and dangerous a chieftain.
But though Galdan was dead the Chinese did not enjoy
that complete immunity from war at the hand of his suc-
cessor that they had looked for. Tse-wang Arabtan was,
however, but the shadow of his brother and predecessor,
and a dispute which arose with the Russians during his
reign weakened his power in other directions. Little Bok-
hara was said to be rich in gold mines, and therefore be-
came a coveted region in the eyes of the Russians. Under
the vigorous administration of Peter the Great an expedi-
tion was despatched to force a passage into the desired
province. To oppose this invasion the Kalmuks assembled
in force, and after a protracted and undecided engagement
the Russians were glad to agree to retire down the Irtish
and to give up all further advance.
To Tse-wang Arabtan succeeded Amursama owing to
the support he received from the Chinese emperor K'een-
lung, who nominated him khan of the Kalmuks and
chief of Sungaria. But, though to the ear these titles
were as high-sounding as those of his predecessors, in
reality the power they represented was curtailed by the
presence of Chinese commissioners, in whose hands rested
the real authority. The galling weight of this state of
dependence drove Amursama before long into revolt. He
dispersed the Chinese garrisons stationed in Hi, kilfed the
generals, and advanced his ovm forces as far as PaUkun on
the river Hi. To punish this revolt, K'een-lung sent a large
force into the rebelHous province. As on the previous occa-
sion, the Chinese were everywhere victorious, and Amursama
fled into Siberia, where he died of smallpox after a short
illness. The Chinese demanded his body, but the Russians
refused to give it up, though they allowed the Chinese
commissioners to identify it. On the death of Amursama,
K'een-lung determined to abolish the khanate, and in place
of it he nominated four Hans to rule over the Simgars, the
TorgoQ, the Khoshod, and the Dorbod. But this divided
authority proved quite as unmanageable as that which had
been wielded by the khan, and the' new rulers soon at-
tempted to throw ofl' the yoke imposed upon them from
Peking. Again a Chinese army marched into Hi, and this
time a severe measure of repression was meted out to the
rebels and their sympathizers. A general massacre of the
Kalmuks was ordered, and was faithfully carried out. The
provinco wliich had been as a fruitful field was utterly
wrecked, and the place of the Sungars was taken by exiled
criminals from China.
But while China was thus absorbing the Mongols within
her reach, Russia was gathering within her borders those
wth whom she came into contact. Among these were
the BuriatB, who occupied a large territory on both fides of
the .Baikal Lake. As usual in such cases, disputes arose
out of distutbauces on the frontiar, and wore ended by
the Buriats and the neighbouring Jlongol tribes becom-
ing one and all tributary to Russia.
Of the Mongol tribes who became entirely subject to The
Russia the principal are those of the Crimea, of Kasan, and p"'*"'
of Astrakhan ; of these the Tatars of Kasan are the truest ^"'^^
representatives of the Golden Horde or Kipchaks, who
originally formed the subjects of Batu and Qlda. Batu,
whose victorious campaign in Russia has airead}' been
sketched, was finally awarded as his fief the vast steppes
which stretch from the Carpathian Mountains to the
Balkash Lake. Over these vast plains the Mongols followed
their flocks and herds, while the more settled among them
established themselves along the banks of the rivers \.hk]x
flow through that region. Batu himself fixed his head-
quarters on the Volga, and there set up his Golden Tent front
which the horde acquired the name of the Golden Horde.
In 1255 Batu died and was succeeded by his brother Bere'':ii-
Khan. During the reign of this sovereign the exactions
which were demanded from the Russian Christians by the
Mongols aroused the Christian world against the barbarian
conquerors, and at the command of Pope Alexander TV. a
general crusade was preached against them. But though
the rage of the Christians was great, they lacked that
united energy which might have availed them against their
enemies ; and, while they were yet breathing out denuncia-
tions, a Tatar host, led by Nogai and Tulabagha, appeared
in Poland. After a rapid and triumphant march, the in-
vaders took and destroyed Cracow, and from thence ad-
vanced as far as Bythom in Oppeln, from which point they
eventually retired, carrying with them a crowd of Christian
slaves. From this time the Mongols became for a season an
important factor in European poUtics. They corresponded
and treated with the European sovereigns, and intermarried
with royal families. Hulagu, the famous general, married
a daughter of Michael Palteologus ; Toktu Khan took as his
wife Maria, the daughter of Andronicus II. ; and to Nogai
Michael betrothed his daughter Irene. But Bereke's in-
fluence extended beyond Europe into Egypt, from which
country, as well as from Constantinople, he secured the
services of artisans to build him dwellings of ja, more
substantial nature than that of his Golden Tent. But his
widely extending intercourse vnih foreign nation^ brought
in its train a consequence which tended fatally to under-
mine the existence of the horde. His conversion to Islam
introduced a strongly disintegrating influence into the com-
munity, and with it were so'svn the seeds of its final dis-
ruption. Bereke was succeeded on his death in J 265 by his
grandson Mangu Timur, who throughout his reign was con-
stantly engaged in hostilities with the Russians and his
other European neighbours. The Genoese alone found under
his patronage a means of advancing their possessions. For
some time these people had held large colonies in southern
Russia, and in the Crimea had divided the trade with the
Venetians. By the .support of Mangu Tinuir these last
were driven out of the field, and the Genoese were left in
the enjoyment of a monopoly of the commerce. The reigns
of the khans who succeeded JIangu Timur were no less
stormy than his had been ; but even in these troublous
times the influences which surrounded the Mongols led
them onward in the path of civilization. Toktu, the next
khan but one to Mangu Timur, is the first Jlongol ruler
whom we hear of as having struck coins. Those issued
during his reign bear the mint marks of Sarai, New Sarai,
Bulgar, Dkek, Kharezm, Krim, JuUad, and Madjarui, and
vary in date from 1291 to 1312.
The adoption of Islam by the rulers of the Golden Horde
had as one result the drawing closer of the relations of
tho Mongols with Constantinople and Egypt. Embassies
[oasscd hitwe^n the three courts, and so important wr.<< the
alliance v.itl; the Mongols deemed by the sultan N.l'<ir
MONGOLS
747
ruler of Egypt, that he sent to aemand in marriage
a princess of the house of Jenghiz Khan. At first his
request was refused by the proud Mongols, but the present
of a million gold dinars, besides a niimber of horses and
suits of armour, changed the refusal into an acquiescence,
and in October 1319 the princess landed at Alexandria in
regal state. Her reception at Cairo was accompanied with
feasting and rejoicing, and the members of her escort were
sent back laden with presents. With that religious tolera-
tion common to his race, Uzbeg Khan, having married one
princess to KAsir, gave another in marriage to George the
prince of Moscow, whose cause he espoused in a quarrel
existing between that prince and his uncle, the grand-
prince Michael. Assuming the attitude of a judge in the
dispute, Uzbeg Khan summoned Michael to appear before
him, and, having given his decision against him, ordered his
execution. The sentence was carried out with aggravated
cruelty in sight of his nephew and accuser. From this
time Uzbeg's sympathies turned towards Christianity. He
protected the Eussian churches within his frontiers, and
put his seal to his new religious views by marrying a
daaghterof the Greek emperor, Andronicus III. He died in
1340, after a reign of twenty-eight years. His coins were
struck at Sarai, Kharezm, Mokshi, Bulgar, Azak, and
Krim, and are dated from 1313 to 1340. His son and suc-
cessor, Tinibeg Khan, after a reign of only a few months,
was murdered by his brother Janibeg Khan, who usurped his
throne, and, according to the historian Ibn Haidar, proved
himself to be "just, God-fearing, and the patron of the
meritorious." These excellent qualities did not, however,
prevent his making a raid into Poland, which was conducted
in the usual Mongol manner, nor did they save his country-
men from being decimated by the black plague, which for
the first time in 1345 swept over Asia and Europe, from
the confines of China to Paris and London. With all their
love of war the Mongols had a keen eye to monetary
advantage, and Janibeg, who was no exception to the rule,
concluded treaties with the merchant-princes of Venice and
Genoa, in which the minute acquaintance displayed with
shipping dues and customs charges shows how great were
the advances the Mongols had made in their knowledge of
European commerce since the days of Jenghiz Khan. The
throne Janibeg had seized by violence was, in 1 357, snatched
from him by violence. As he lay ill on his return from a
successful expedition against Persia he was murdered by
his son Berdibeg, who in his turn was, after a short reign,
murdered by his son Kulpa. With the death of Berdibeg
the fortunes of the Golden Horde began rapidly to decline.
As the Uzbeg proverb says, — " The hump of the camel was
cut off in the person of Berdibeg."
The But while the power of the GSolden Horde was dwin-
\vuie dling away, the White Horde or Eastern Kipchak, which
^j"^'^ was the inheritance of the elder branch of the family
j;^grn '^ Juchi, remained prosperous and full of vitality. The
Kipcbak. descendants of Orda, Batu's elder brother, being far re-
moved from the dangerous influences of European courts,
maintained, much of the simplicity and vigour of their
nomad ancestors, and the throne descended from father
to son with undiminished authority until the reign of
Urus Khan (1360), when complications arose whichchanged
the fortunes of the tribe. Like many other opponents of
the Mongol rulers, Khan Tuli Khoja paid with his life for his
temerity in opposing the political schemes of his connexion
Urus Khan. Toktamish, the son of the murdered man,
fled at the news of his father's death and sought refuge at
the court of the famous Timur-i-leng (Tamerlane), who
deceived him with honour and at once agreed to espouse
his causa. With this intention he despatched a force
againtt Vr.'-i Khc.n, and gained some advantage over him,,
but, while Citing out another army to make a fresh attAck,
news reached him of the death of Urus. Only at Sighnak
are coins known to have been struck during the reign of
Urus, and these bear date from 1372 to 1375.
He was followed on the throne by his two sons, Tuk-ToV-
takia and Timur Malik, each in turn ; the first reigned but tamisV
for a few weeks, and the second was killed in a battle
against Toktamish, the son of his father's enemy. Tok-
tamish now seized the throne, not only of Eastern Kipchak
but also of the Golden Horde, over which his arms had
at the same time proved victorious. His demands for trib-
ute from the Russian princes met with evasions from men
who had grown accustomed to the diminished power of the
later rulers of the Golden Horde, and Toktamish therefore
at once marched an army into Russia. Having captured
Serpukhoff, he advanced on Moscow. On the 23d August
1382 his troops appeared before the doomed city. For
some days the inhabitants bravely withstood the constant
attacks on the walls, but failed in their resistance to the
stratagems which were so common a phase in Mongolian
warfare. Wi.L astonishing credulity they opened the gates
to the Mongols, who declared themselves the enemies of
the grand-prince alone, and not of the people. The usual
result followed. 'The Rus.sian general, who was invited to
Toktamish's tent, was there slain, and at the same time the
signal was given for a general slaughter. Without dis-
criminating age or sex, the Mongol troops butchered the
wretched inhabitants without mercy, and, having made
the streets desolate and the housis tenantless,-they first
plundered the city and then gave it over to the flames.
The same pitiless fate overtook Vladimir, Zvenigorod,
Yurieflf, Mozhaisk, and DimitroflT. With better fortune,
the inhabitants of Pereslavl and Kolomna escaped with
their lives from the troops of Toktamish, but at the expense
of their cities, which were burned to the ground. Satisfied
with his conquests, the khan returned homewards, travers-
ing and plundering the principality of Eiazan on his way.
Flushed with success, Toktamish demanded from his patron
Timur the restoration of Kharezm, which had fallen into
the hands of the latter at a period when disorder reigned
in the Golden Horde. Such a request was not likely to
be well received by Timur, and, in answer to his positive
refusal to yield the city, "Toktamish marched an army of
90,000 men against Tabriz. After a siege of eight days
the city was taken by assault and ruthlessly ravaged.
Meanwhile Timur was collecting forces to punish his
rebeUioiis protige. When his plans were fully matured, ho
advanced upon Old Urgenj and captured it. More merci-
ful than Toktamish, he transported the inhabitants to
Samarkand, but in order to mark his anger against the
rebellious city he leveOed it with the ground and sowed
barley on the site where it had stood. On the banks of
the Oxus he encountered his enemy, and after a bloody
battle completely routed the Kipchtis, who fled in confu-
sion. A lull followed this victory, but in 1390 Timur
again took the field. To each man was given "a bow,
with thirty arrows, a quiver, and a buckler. The army was
mounted, and a spare horse was supplied to every two men,
while a tent was furnished for every ten, and with this
were two spades, a pickaxe, a sickle, a saw, an axe, an awl,
a hundred needles, 8i ft) of cord, an ox's hide, and a strong
pan." Thus equipped the army set forth on its march.
After a considerable delay owing to an illness which over-
took Timur his troops arrived at Kara Saman. Here
envoys arrived from Toktamish bearing presents and a
message asking pardon for his past conduct ; but Timur
was inexorable, and, though he treated the messengers with
consideration, he paid no attention to their prayer. In
face of innumerable diflSculties, as well as of cold, himger,
, and weariness, Timur marched forward month after month
I through the Kipchak country in pursuit of Toktamish. At
748
MONGOLS
last, on the 18th of June, he overtook him at Kandurcha, I One solitary fragment of the Golden Horde, the khanat
in the country of the Bulgars, and at once forced him to an of Astrakhan, maintained for a time an existence after th
encao-ement. For three days the battle lasted, and after
inclining now to this side and now to that victory finally de-
cided in favour of Tiraur. The Kipchaks were completely
routed and fled in all directions, while it is said as many
as 100,000 corpses testified to the severity of the fighting.
Timur pursued his flying enemy as far as the Volga,
slaughtering all who fell into his hands, and ravaged and
destroyed the to\vns of Sarai, Saraichuk, and Astrakhan.
Having inflicted this terrible blow on the Golden Horde,
Timur distributed rewards to his chieftains, and presided
at a series of banquets in celebration of his victory. These
rejoicings over, he returned to Samarkand laden with spoils
and trophies. But Toktamish, though defeated, was not
subdued, and in 1395 Timur found it necessary again to
undertake a campaign against him. This time the armies
met upon the Terek, and after a fiercely-contested battle
the Kipchaks again fled in confusion. When the victory
was gained, Timur, we are told, knelt down on the field
and returned thanks to Heaven for his success. The piu--
suit along the Volga was vigorously undertaken, and the
slaughter among the fugitives was terrible. The hurried
advance of Timur's horsemen threw the Russians into a
state of wild alarm, and the grand-prince of Moscow
ordered that an ancient image of the Virgin which was
lielieved to possess miraculous power should be talcen to
Moscow to save that city from the destroyer. Success
appeared to attend this measure, for Timur, threatened by
the advancing autumn, gave up all further pursuit, and
retired with a vast booty of gold ingots, silver bars, pieces of
Antioch linen and of the embroidered cloth of Russia, &c.
On his homeward march southwards he arrived before
Azak, which was then the entrepot where the merchants
of the east and west exchanged their wares. In vain the
natives, with the Egyptian, Venetian, Genoese, Catalan,
and Basque inhabitants, besought him to spare the city.
His answer was a command to the Moslems to separate
themselves from the rest of the people, whom he put to
the sword, and then gave the city over to the flames.
Circassia and Georgia next felt his iron heel, and the
fastnesses of the central Caucasus were one and all
destroyed. After these successes Tiraur gave himself up
for a time to feasting and rejoicing, accompanied by every
manifestation of Oriental luxury. " His tent of audience
was hung with silk, its poles were golden, or probably
covered with golden plates, the nails being silver ; his
throne was of gold, enriched with precious stones ; the
floor was sprinkled with rose water." But his vengeance
was not satisfied, and, having refreshed his troops by this
halt, ho marched northwards against Astrakhan, which he
utterly destroyed. The inhabitants were driven out into
the country to perish with the cold, while the commander
of the city was killed by being forced beneath the ice of
the Volga. iSarai nest shared the same fate, and T.imur,
having thus crushed for the' second time the empire of
Toktamish, set out on his return home by way of Derbend
and Azerbijan. The defeated Idian succeeded shortly
.afterwards in recaphiring Sarai ; but, being again driven
out, ho retired in 1393 to Kieff, a fugitive from his king-
dom. During his reign, which lasted for twenty-four years,
lie strack coins at Kharezm, Krim, New Kri;n, Azak,
Sarai, New Sarai, Saraichuk, and Astrakhan. The power
in the hands of the successors of Toktamish never revived
after the last campaign of Timur. They were constantly
engaged in wars with the Russians and the Xrim Tatars,
with whom the Russians had allied themselves, and by
degrees their empire decayed, until, on tho seizure and
death of Ahmed Khan at the beginning of the ICth cen-
tury, the domination of the Golden Horde camo to an end.
fall of the central power. But even this last remnar
ceased to be a Mongol apanage in 1554, when it wi
captured by the Russians and converted into a Russiai
province. The fate which thus overtook the Golden Hord
was destined to be shared by all the western branches oi
the great Mongol family. The khans of Kasan and
Kasiinoff had already in 1552 succumbed to the growing
power of Russia, and the Krim Tatars were next toTbe
fall under the same yoke. In the ISth century, whenj^'''t
the Krim Tatars first appear as an independent power,
they attempted to strengthen their position by allying
themselves \vith the Russians, to whom they looked for
help against the attacks of the Golden Horde. But while
they were in this state of dependence another power arose
in eastern Asia which modified the political events of that
region. In 1453 Constantinople was taken by the
Osmauli Turks, who, having quarrelled with the Genoese
merchants who monopolized the trade on the Euxine, sent
an expedition into the Crimea to punish the presumptuous
traders. The power which had captured Constantinople
was not likely to be held in check by any forces at the
disposal of the Genoese, and without any serious opposi-
tion Kaffa, Sudak, Balaclava, and Inkerman fell before the
troops of the sultan Mohammed. It was plain that,
situated as the Crimea was between the two great powers
of Russia and Turkey, it must of necessity fall under the
direction of one of them. AVhich it should be was
decided by the invasion of the Turks, who restored Mengli
Girai, the deposed khan, to the throne, and virtuafiy
converted the khanate into a dependency of Constanti-
nople. But though under the tutelage of Turkey, Mengli
Girai, whose leading policy seems to have been the desire
to strengthen himself against the khans of the Golden
Horde, formed a close alliance with the grand-prince Ivan
of Russia. One result of this friendship was that the
Mongols were enabled, and encouraged, to indulge their
predatory habits at the expense of the enemies of Russia,
and in this way both Lithuania and Poland suffered
terribly from their incursions. It was destined, however,
that in their turn the Russians should not escape from
the marauding tendencies of their allies, for, on pretext
of a quarrel with reference to the succession to the Kasan
throne, Mohammed Girai Khan in 1521 marched an army
northwards until, after having devastated the country,
massacred the people, and desecrated the churches on his
route, he arrived at the heights of Vorobieff overlooking
Moscow. The terror of the unfortunate inhabitants at
tho sight once again of the dreaded Mongols was extreme ;
but the horrors which had accompanied similar past
visitations were happily averted by a treaty, by which
the grand-prince Vasili undertook to pay a perpetual trib-
ute to the krim khans. This, however, proved but a truce.
It was impossible that an aggressive state like Russia shovdd
live in friendship vdth a marauding power like that of the
Krim Tatars. Tho primary cause of contention was the
khanate of Kasan, which was recovered by the Jlongols,
and lost again to Russia with that of Astralchan in 1555.
The sultan, however, declined to accept this condition of
things as final, and instigated Devlet Girai, the Krim
khan, to attempt their recovery. With this object the
latter marched an army northwards, where, finding the road
to Moscow unprotected, ho pushed on in the direction of
that ill-starred city. On arriving before its walls he found
a large Russian force occupying tho suburbs. With these,
however, ho was saved from an encounter, for just as his
foremost men approached the town a fire broke out,'
which, in consci|Utnco of tho high wind blowing at the
time, spread with frightful rapidity, and in the spaco
MONGOLS
749-
of six hours destroyed all the churches, palaces, and
houses, with the exception of the Kremlin, within a
compass of 30 miles. Thousands of the inhabitants
perished iu the flames. "The river and ditches about
Moscow," says Horsey, " were stopped and filled with the
multitudes of people, laden with gold, silver, jewels,
chains, ear-rings, and treasures. So many thousands were
there burned and drovmed that the river could not be
cleaned for twelve months afterwards." Satisfied with
the destruction he had indirectly caused, and unwilling to
attack the Kremlin, the khan withdrew to the Crimea,
ravagLug the country as he went. Another invasion of
tussia, a few years later (1572), was not so fortunate for
ho Mongols, who suffered a severe defeat near Molody,
•I versts from Moscow. A campaign against Persia made
diversion in the wars which were constantly waged
eiweea the Krim khan and the Russians, Cossacks, and
Poles. So hardly were these last pressed by their per-
inacious enemies in 1649 that they bound themselves
)y treaty to pay an annual subsidy to the khan. But
;he fortunes of war were not always on the side of the
Tatars, and with the advent of Peter the Great to the
Russian throne the power of the Krim Mongols began to
decline. In 1696 the czar, supported by a large Cossack
force under Mazeppa, took the field against Selim Girai
Khan, and gained such successes that the latter was
compelled to cede Azoff to him. By a turn of the wheel
of fortune the khan had the satisfaction in 1710 of
having it restored to him by treaty ; but this was the last
real success that attended the Tatar arms. In 1735 the
Russians in their turn invaded the Crimea, captured the
celebrated lines of Perekop, and ravaged Baghchi Serai,
the capital. The inevitable fate which was hanging over
the Krim Tatars was now being rapidly accomplished.
In 1783 the Krim, together with the eastern portion of
the land of the Nogais, became absorbed into the Russian
province of Taurida.
Another branch of the Mongol family which requires
mention is that of the Kazaks (see Kirghiz, vol. xiv. pp.
95, 96), whose ancient capital was Sighnak, which, as we
have seen, passed into the hands of the great Timur. It
will now only be necessary to refer briefly to the Uzbegs,
who, on the destruction of the Golden Horde, assumed an
important position on the east of the Caspian Sea. The
founder of their greatness was the khan Abulkhair, who
reigned in the 15th century, and who, Hke another Jenghiz
Khan, consolidated a power out of a number of small clans,
and added lustre to it by his successful wars. Sheibani
Khan, his grandson, proved him^self a worthy successor, and
a doughty antagonist of the great Moghul emperor Baber.
In 1500 he inflicted a severe defeat on Baber's forces, and
captured Samarkand, Herat, and Kandahar. By these and
other conquests he became possessed of all the country be-
tween the Oxus and the Jaxartes, of Ferghana, Kharezm,
and Hissar, as well as of the territory of Tashkend from
Kashgar to the frontiers of China. In the following year,
by a dashing exploit, Baber recovered Samarkand, but only
to lose it again a few months later. During several succeed-
ing years Sheibani's arms proved victorious in many fields
of battle, and but for an indiscreet outrage on the terri-
tories of the shah of Persia he might have left behind him
a powerful empire. The anger, however, of Shah Ismael
roused against him a force before which he was destined
to falL The two armies met in the neighbourhood of
Merv, where, after a . desperate encounter, the Uzbegs
were completely defeated. Sheibani, with a few followers,
sought refuge in a cattle-pound. But, finding no exit on
vhe farther side, the refugees tried to leap their horses
over the wall. In this attempt Sheibani was killed.
iWhen his body was recognized by his exultant enemies
they cut off the head and presented it to the shah, who
caused the skull to be mounted in gold and to be converted
into a drinking-cup. After this defeat the Uzbegs withdrew
across the Oxus and abandoned Khordsiu. Farther east the
news aroused liuber to renewed activity, and before long
he reoccupied Sani.irkand and the province " Beyond the
River," which had been dominated by the Uzbegs for nine
years. But though the Uzbegs were defeated, they were by
no means crushed, and ere long we find their khans reigning,
now at Samarkand, and now at BokharaT As time advanced
and European powers began to encroach more and more
into Asia, the history of the khanates ceases to be confined
to the internecine struggles of rival khans. Even Bokhara
was not beyond the reach of Russian ambition and English
diplomacy. Several European envoys found their way
thither during the first half of the present century, and
the murder of Stoddart and Connolly in 18-12 forms a
melancholy episode in British relations with that fanatical
capital. W/^ the absorption of the khanate of Bokhara
and the capture of Khiva by the Russians the individual
history of the Mongol tribes in Central Asia comes to an
end, and their name has left its imprint only on the dreary
stretch of Chinese-owned country from Manchuria to the
Altai Mountains, and to the equally unattractive coimtry
in the neighbourhood of the Koko-nor. (e. k. d.)
Lair^iuage and LiUratiirc. — The Mongol tongue is a nicmtcr of
the great stock which recent scholars designate as Finno-Tataric or
Ural-Altaic, which comprehends also the languages of the Txuigoos
(Manchu), Tuiko-Tatars, Finns, and Samoyeds. The members of
this group are not so closely related to one another as those of the
Indo-European stock ; but they are all hound together by the com-
mon principle of agglutinative formation, especially the so-called
hannony of vowels, by their grammatical structure, and also by-
certain common elements in the stock of roots which run through
thera all, or through particular more closely-connected families
within the group. ^
The fatherland proper of the Mongols is the so-called Mongolia.
It stretches from Sibei-ia in the north towards the Great Wall of
China in the south, from Dauria and Manchuria in the east to the
Altai and the sources of the Irtish, Thian-shan (i.^., heaven moun-
tains), and East Turkestan in the -west. In the centre of this
country is the desert of Gobi (Chinese Sha-mo, i.e., sand-sea). The
Mongolian population, however, extends in the south over the Grcit
Wall to the basin of the Kbkb-nor (blue lake), and thence extends
due west over Tangut and the northern border of Tibet. Crossing
the political frontier, we find Mongols in the Russian province
Turkestan, in the territories of Semiryetshensk (land of the seven
streams), Alatau, and Semipalatinsk in the west, in the south of
the province of Tomsk, with a more populous region due north in
Siberia, round the Baikal Lake. The country north of the Gobi,
from the Altai, Tangnu, and the Saian mountains iu the .west to
Manchuria in the east, is called Ehalkha, with the chief distiicts
Urga (Kure), Uliassutai, Khobdo (Kobdo). In a north-westerly
direction from Gobi, bet^veen Thian-shan and the Altai, is Sungaria.
The sum total of the Mongol population under Chinese government
is calculated at between two and three millions.
Generally the whole Mongol ti-ibe may be divided into three
branches : East Mongols, West Mongols, and Buriats.
(1) The East Mongols are divided into the Khalkhas in the
borders just mentioned, the Shara Mongols south of the Gobi along
the Great Wall north-eastward to Manchuria, and lastly the Shii-
aigol or Sharaigol in Tangut and in northern Tibet.
(2) On the signification and employment of the difierent names
of the West Mongols (Kalmuks, Oelbd, Oirad or Dorbiin Oirad = the
foiu- Oirad, Mongol Oirad), and also as regards the subdivision of the
tribes, there is much uncertainty. The name Kalmuk, so generally
employed among us, is in fact only used by the Volga Kalmuks
(Khalimak), but even with them the name is not common, and
almost a bj-name. It is of foreign origin, and most likely a Tataric
word which has yet to be explained. Oirad means the "near
ones," the "related." The usual explanation given is that the
single tribes consider themselves as being related to each other, —
hence Mongol Oirad, "the Mongol related tribe." This is the
favoui-ite name among Kalmuks. Dbrbbn Oira J, or the four related
tribes, comprise (1) Sungars, (2) Torgod, (3) Khoshod, (i) Dorbbd.
' Compare W. Schott, Versuch iiber die tatarischcn Spradicn (Berl.,
1886), Ueber das altaCsche od^rjinn^jch-tatarisc/ie SprachengeschUchi
(Berl., 1849), Aitajische Sliiditn, P.nrts i.-v. (Berl., 1860-1870); and
A. Gastrin, Ethnologische Vorlesungen iiber die Altai'schen Votker;;
edited by A. Schiefhet (Fetersb., 18i7).
750
M O I^ Ci O L S
The signification of the name Oeldd, in the East Mongolian Ocgelcd,
now the most widely spread amonc; the tribes living in China, is
iikewiie very doubtful. Some assert that '* Oelod" is nothing but
the Chinese transcription of Oirad, as the ordinary Chinese language
does not possess the sound r. We have, however, to bear in mind
that we have a Mongolian root Ogelekii, with the sense "to be in-
imical," " to bear hatred, ill-will," &c. The main population of the
Kalmuks live, or rather drag out, their existence after the usual
fashion of nomad tribes in Sungaria, in the eastern part of the Thian-
shan, on the south border of the Gobi, on Kokd-nor, and in the
province of Kan-suh. All these are under the Chinese Government.
In consequence, however, of the extension of the Russian empire
in Thian-shan and Alatau, many hordes have come under the Rus-
sian sway. According to an approximate account we may reckon
in the tcmtory Semiryetshensk (Kuldja) and Semipalatinsk 34,000
Kalmuks, while in the southern part of the government Tomsk,
on the Altai, the Kalmuk population amounted formerly to 19,000.
Besides these we find a section of Kalmuk population far in the
west, on the banks of the Volga (near Astrakhan). From their
•original seats in Sungaria they turned in their migrations to the
north, crossed the steppe of the Kirghiz, and thus gradually reached
the Emba and the Or. Between these two rivers and the Ural the
Torgod settled in 1616 ; thence they crossed the Volga in 1650,
and took possession of the now so-called steppe of the Kalmuks,
being followed in 1673 by the Dorbbd, and in 1675 by the Khoshod.
In 1771 a considerable number returned to the Chinese empire.
At the present time there is a not unimportant population in the
so-called steppe of the Kalmuks, which extends between the Caspian
and the Volga in the east and the Don in the west, and fiom the
town of Sarepta in the north to the Kuma and the Manytch in
the south. According to modern statistical accounts, this popula-
tion amounts to 75,630. To these we have to add 24,603 more on
the borders of the Cossacks of the Don, and lastly 729S in the
bordering provinces of Orenburg and Saratoff. The sum total of
the so-called Volga Kalmuks is therefore 107,531.
(3) In the southern part of the Russian province of Irkutsk,
in a wide circle round the Baikal Lake, lies the heirdom proper of
the Buriats, which they also call the "Holy Sea;" the country
east of the lake is commonly called Transbaikalia. Their country
practically extends from the Chinese frontier on the south within
almost parallel lines to the north, to the to\\'n Kirensk on the Lena,
and from the Onon in the east to the Oka, a tributary of the Angara,
in the west, and still farther west towards Nijni-Udinsk. They
are most numerous beyond the Baikal Lake, in the valleys along
the Uda, the Onon, and the Selenga, and in Nertchinsk. These
Trans- Baikalian Buriats came to these parts only towards the end
of the 17th century from the Khalkhas. While Mongols and Kal-
muks generally continue to live after the usual fashion of nomads,
, we find here agricultural pursuits, most likely, however, due mainly
to Russian influence. Christianity is also making its way. The
sum total of the Buriats amounts at present to about 250,000,
Another tribe separated from the rest of the Mongols is the so-
called Hazara (the thousand), and the four Aimak {i.e., tribes),
who wander about as herdsmen in Afghanistan, between Herat and
Kabul. In external characteristics they are Mongols, and in all
probability they are the remains of a tribe from the time of the
Mongol dynasty. Their language, which shows, of course, Persian
influence, is strictly Mongolian, more particularly West ilongolian or
Kalmuk, as baa been proved by H. C. von der Gabelentz.^
Agreeably with this threefold division of the Mongols we have
-alo a threefold division of their respective languages: (1) East
Mongolian or Mongolian proper, (2) West Mongolian or Kalmuk,
(3) Buriatic.
The dialects just mentioned are found to be in close relation to
each other when wc ejramine their roots, inflexions, and grammatical
structure. The difl"erenc6 between them is indeed so slight that
whoever understands one of them understands all. Phonetically a
characteristic of them all is the "harmony of vowels," which are
divided into two chief classes : the hard a, o, u ; and the soft e, i>, U \
between which i is in the middle. All vowels of the same word
must necessarily belong to the same class, so that the nature of the
first or root-vowel determines the nature of the other or inflexion-
vowels ; now and then a sort of retrogressive harmony takes place,
60 that a later vowel determines the nature of the former. The
■consonants preceding the vowels are equally under their influence.
The Mongolian characters, which in a slightly altered form are
also in use among the Manchus, are written perpendicularly from
above downward, and the lines follow from left to right, the aljAa-
bet having signs for seven vowels a, c, i, o, u, d, U, and diphthongs
derived from them ao, ai, ei, ii, oi, ui, 6i, i/i, and for seventeen con-
Bonants n, 6, k/i, gh, k; g, m, I, r (never initial), t, d, y, s ((/s), ts,
S3, ah, to. All these are moJiflod in shape accoi-ding to thoirposirion,
in the beginning, miildlo, or end of a word, and also by certain
orthographic rules. In Mongolian and Manchu writing tho syllable
(t.<., the consonant together with tho vowel) is considered as a unit.
in other woids, a syllabarium rather than an alphabet. The exist-
ing characters are hneal doscendanta of the original Uigurian forms,
which were themselves derived from the Syriac, having been brought
to the Uigurs by Nestorian missionaries. An Indian and Tibetan
influence may also be noticed, while the arrangement of the char-
acters in perpendicular lines is common to the Chinese. The sit-
ing was brought into its present shape by the learned Larnas Sa-
skya Pandita, Phags-pa Lama, and Tshoitshi Odser in the 13th
century,^ but is exceedingly imperfect. To express the frequently-
occurring letters boiTowed from Sanskrit and Tibetan, ■which are
-wanting in the Mongol alphabet, a special alphabet called Gallk
is employed. Every one who has tried to read Mongolian knows
how many difficulties have to be overcome, arising fiom the ambi-
guity of certain letters, or from the fact that the same sign is to
be pronounced differently according to its position in the word.
Thus, there are no means for distinguishing the o and «, 5 and H,
the consonants g and k, t and d, ;/ and s [ds). A and c, o (u) and
0 {U), a (f) and n, g and kh, t {d.) and on, are liable to be mistaken
for each other. Other changes will be noticed and avoided by
advanced students. It is a great defect that such common wordi
as ada (a fury) and cnde (here), emde (here) and nada (me), aldan
(fathom) and altan (gold), (rrdic (court-residence) and nrlic (long),
onokhu (to seize) and unukku (to ride), tere (this) and dere (pillow^,
yebe (said) and kcbc (made), gem (evil) and kern (measure), gcr (house)
and ker (how), naran (sun) and nere (name), yagon (what) and
dsagon (hundred), should be written exactly alike. This list might
be largely increased. These defects apply equally to the Mongolian
and Buriatic alphabets.
In 1648 the Saya Pandita composed a new alphabet (the Kalmuk),
in which these ambiguities are avoided, though thegraphic differences
between the two alphabets are only slight. The Kalmuk alphabet
avoids the angular and clumsy shapes of the Mongolian, and has,
on the contrary, a rounded and pleasing shape. The Kalmuk
alphabet has also this great advantage, that every sound has its
distinct graphic character ; a mistake between two characters can
scarcely occur. The Kalmuk words once mastered, they can be
easily recognized in their Mongolian shape. The dialectical differ-
ences are also very slight.
The Kalmuk, therefore, is the key of the Mongolian, and should
form tho groundwork of Mongolian studies. The Kalmuk and East
Mongolian dialects do not differ much, at least in the spoken language ;
but the Kalmuks WTite according to their pronunciation, while the
Mongols do not. For example, son (c?se7t), "nundred," is pronounced
alike by the Kalmuks and the East Mongolians ; but according to
Mongolian orthography the word appears in the form dsagcn. The
dial*";tic difference between the ti\o dialects very frequently lies
only in a different pronunciation of some letters. Thus East Mon-
golian fis is in Kalmuk soft s, &c. The chief difference between the
two dialects lies in the fact that in Kalmuk the soft guttural g be-
tween t\vo vowels is omitted, while, through the joining of the two
vowels, a long vowel is produced. In the pronunciation of common
East Mongolian tho g is likewise omitted, but it is written, while
in Kalmuk, as just now mentioned, the guttural can only be trace^l
through the lengthening of the syllable. Thus we find : Mongol
khagan, "prince," Kalmuk kkdn ; M. dagon, "voice, sound," K.
doll, dun ; M. dologan, " seven 'VK. dolon ; M. agola, "mountain,"
S. 5ia, ula ; M. nagor, "lake, ' K. ndr^ niir ; M. ulagan, "red,"
K. iildn; M. yagon, "what,"K. ydn{yii7i); M. rfaJa^-rtn, "mountain-
ridge," K. dabdn ; M. ssanagan, " thought," K. ssandn ; M. baragov,
" on the right," K. baron, barun ; M. shibagon, " bird," K. showdn ;
M. chilagon, "stone," K. chUdn (chuIilJi) ; M. Jirgogan, "six," K.
surgdn; M. dcgcre, "high, above," K. dere; M. ugiikhu, "to drink,"
K. ukhu; M. togodshi, "history," K. todshi, tudshi; M. cgildcn,
"door," K. oden; M. dsegiin, "left," K. s6n; M. Ggede, "in the
height," K. 6di) ; M. ^gded, "the Kalmuks," K. olod ; M. ilileged,
"if one has done," K. iliUd; M. kabegiin, "son," K. kiiit-dn ; M.
gcgiin, ".mare," K. g^n\ M. kcgUr, "corpse,"K. k-ur; M. kharigad,
"returned," K. khared, &c.
Tho Buriatic, in these peculiarities, is almost always found with
East Mongolian, with which it is in every respect closely allied.
In the pronunciation of some letters the transition of East Mongolian
Ua, ise into Buriatic ss is noticeable ; for instance : Mong. tsetsek,
"flower," Buriatic ssessek ; M, tsak, "time," B. ssak ; M. tsagan,
"white," B. s.'iagan ; M. tsdscn, "prudent," B. sscsscn. Ss is some-
times pronounced like (the German) ch: East M. ssain, "good," B.
chain; M. sscdkil, "heart," B. chedkil, K in the beginnin;; or
middlo of a word is always a^piratciL
The noun is declined by the help of appended particles, some of
which are independent post-positions, viz., Gen. ytn, u, un\ Dat.
rf^ir, a ; Ace. yi, i ; Ablat else ; lustrum, bcr, ycr ; Associative,
htga, luge. The dative and accusative have also special forms which
have at the same time a possessive sense, viz., Dat dagan, dcgen ;
Accus. ben, yen. Tho plural is expressed by affixes (naj; ner, od,
ss, d), or freauently by words of plurality, "all," "many," c.g.^
kilmiin nog6d (man, many^mi-n). Tho oblique cases have the
» Cf. H. C. von dcr GabelcDti, in the Zcitachrifl /. d. Kundt d. JtfMyfn?nfid<j
O^ttingeD, 1838, vol U. pp. 1-21, "Versucb ubereinealtemoagoUsobeliischrlft.'
M O N — M O N
761
•une en(UQg9 in eingular and plural. Gender is not indicated.
The adjective is uninflected both as attribute and as predicate ;
there is no comparative form, this idea being expressed by the con-
struction or by the use of certain particles. The personal pronouns
an bi, I ; tchi, thou ; bida, we ; ta, ye ; their genitives serve &s pos-
Mssives. The demons tratives are en«, Ure (this, that), plural ede^
Ude ; interrogative ken^ who ! The reUtive is lacking, and its place
is supplied -by circumlocutions. The numerals are : 1, nigen ; 2,
khoyar ; 3, gurhan ; 4, dSrben ; S, tabun ; 6, jirgugan ; 7, dologan \
8, naiTTtan; 9, yisun \ 10, arban ; 100, dsagon ; 1000, minggan.
The ordinals are formed by appenthng tugar, tiiger. The theme of
the verb is seen in the imperative, as bari, grasp. The conjugation
is rich in forms for tense and mood, but person and number are with
few exceptions unexpressed. The present is formed from the theme
by adding mui {barirmii), the preterite by bai or luga (baribai, bari-
luga), the future by ssugai or asu (barissugai, barissu). The preterite
has also in the third person the terminations dsugui and run ; the
future has in the third person yu, and in the first ya. The con*
ditional ends in bassu ifiarxbassu), the precative in tugai, tiigei,
the potential in $a {bariTnuUa), the imperative plural in ktxtn, the
gerund in the present in n, dsu {barin, baridsu) or tala, "while, till "
{bariiala^ "inter capiendura"), in the preterite it is formed in gad
{barigad) ; the present part, has ktchi [bai^tchi), the past part.
kssan {barikssar.) ; the supine ends in ra, the infinitive in khu
{barikhii, or when used substantively barikhui). Ther« is but one
perfectly regular conjugation, and derivative forms, derived from
the theme by infixes, are conjugated on the same scheme. Thus
the passive has infixed ta or kSi {barikdakhu, to be grasped), the
causative gul {barigulkhu, to caxise to grasp), the co-operative or
sociative Usa or Ida (barillsakhu, to grasp together).
There are no prepositions, only post-positions. Adverbs are either
simple particles (affirmative, negative, interrogative, mod^d, kc),
or are formed by suffixes from other parts of crieech. There are
Ter^ few conjunctions ; the relations of clauses and sentences are
mainly indicated by the verbal forms (part., sup., conditional, but
mainly by the gerund).
The order of words and sentences in construction is pretty much
the opposite of that which wo follow. In a simple sentence the
indication of time and place, whether given by an adverb or a sub-
stantive with a post-position, always comes lirst ; then comes the
subject, always preceded by its adjective or genitive, then the object
and other cases depending on the verb, last of all the verb itself
preceded b/ any adverbs that belong to it So in the structure of
a period all causal, hypothetical, concessive clauses, which can be
conceived as preceding the main predication in point of time, or
even'as-contemporary with it, or as in any way modifying it, must
come first ; the finite verb appears only at th* end of the main
predication or apodosis. The periods are longer than in other
languages ; a single one may fill several pages.
Grmmmara and dictionaries may be divided according to the three dialect*.
For East Mongolian, I. J. Schniidt gave the first grammar (I'etersb., 1831X aod
aMongolfan-Gcrman-RussiaQ dictionary(Pctersb., 1835). Next Joa. Kowalewsld
publianed ia Russian a iiongoIiaD grammar (Kasan, 1835X a chrestomathy (2
Tola., KAcan, 1836, 1837), and iiisgreat Di<iionnair»inofiyoI-rM«.fran^u(3 vols.,
KasAD, 1S44, 1840, 1349). We came also R. Tuille, Short Mongolian Grammar
<in MonpolianX xylographed at the mission press near Bselenginsk beyond Lake
Baikal (1833). A. BobrowBikow's Rusaian Grammar o/ ths Mongolian-Kalmvk
Langvagt (Kasan, 1849) is also very good. An abridgment of Schmidt's work
ia C. Puini, EUmenti della fframmatica mongolica (Florence. 1878). A. Popow'a
Mongolian C7ir«X<wn<UAv appearert in 2 vols, at Kasan (1836). For the KaJmuk
we have grammars by Popow iKaaan, 1847), Bobrownikow aa above, and H. A.
Zwick (i. I. tt a.), autographed at Donaaeschingen (1861). Zwick'a autographed
Kalmuk and Oerman dictionary with a printed German index appeared (i. {.
tl a.) in K62 ; B. JUlg's edition of the tales of Siddbl-kQr (Leips., 1866) gives
a complete glossary to these stories. There are small Russian and Kalmuk
Tocabuloriu by P. Smirnov (fiLasan, 1857} and C. Qolstonskyi (Petersb., 18G0}.
atic coUoqoial language (Kasan, 1878).
HUTaiurt.—A clear distinction must be drawn between tlie higher and noblw
written or book-la ngiiage and the common or conversational language of every-
day life. The difference between the two is very considerable, and may b«
foirly compared to that between the Modem High German book-language and
th9 different dialects. AU grammars and dictionaries as yet published treat
only of the book -language ; and so also, with a few exceptions, the publlahed
literary documents arc written^in this higher style. The exceptions are tbs
Gesser-Khan, and the Siddhi-kur and Djangariad (the last two published by
GolstuDskyi). The popular or conversational language has only quite lately been
fixed in writing by A. Pordnyeyew in his Russian work, Speciment o/ tht Popular
LUtToXurt of the Mongolian THbe$, part I., " Popular Songs" (Petersb., 1880X
which contains rich material for the study of the popular literature.
The literature known at present consists mostly of translations from the
Tibetan, the holy language of Buddhism, which is still the language of the
learned. The Tibetan Buddhist literature is itself translated from the Banskrit I
hence, now and then, through Mongols and Kalmuks we get acquainted with
Indian works the originals of which are not known in Sanskrit Such Is the
case, for instance, with the tales of Siddhi-kllr. Many b<]oks have also been
translated from the Chinese. Most of the writings are of a religious, historical,
philosophical, medical, astronomical, or astrological character. Favourite sub-
jects are folk-lore and fairy tales. Amonff the religious books, perhaps the most
important Is that containing the legenda entitled iiliger iin dalai, "ocean of
comparisons" (edited by the late I. Jacob Sclimidt under the title, Dtr iVeiM
vtid der Thor, in Tibetan and German, Petersb., 1843). To this may be added
the boddhi mor, or " the holy path," the altan gtrtl, "gleaming of gold," tbs
tiiani gamix), and yeriiintchii yin toH, " mirror of the world." What was known
of poetical lit^'-ratnre before Pozdnyeyew is scarcely worth mentioning, la
some parte of v^ac Historical and narrative literature we find, wherever the nar-
rative takes a higher flight, an admixture of poetical diction. The poetry
appears in a certain parallelism of the phrases, with a return eitiier of the
same endings (rhyme) or of the same words (refrain). Frequently we find,
besides the rhyme or relVain. alliteration. The essay of H. C. von^der Qabeleatz
in Z. / d. KuTide da Morgeniandts, vol. i. pp. 20-37, " Einiget Uber Mongoliache
Poesie," has been superseded by the work of Pozdnyeyew.
Among historical works a high place is due to that composed by the tribal
prince, Ssanang Ssetsen, in the middle of the 17th century {Geschichte dtr Ott-
Mongolen und tkra Fiirttenhavaa, Mong. and Germ., by I. J. Schmidt, Petereb.,
1829X and to the Altan tobtchi, i.e., " Golden knob " or " precious contents "
(text and Russian translation by the Lama Oalsang Gomboyew, Petersb.,
1858). Of folk-lore and fairy tales, we have the legend of the hero Cess€r^
KJian (text ed. by I. J. Schmidt, Petersb., 1836. and German version. 1839 ; comp.
Schott. Ueberdie Sags v. Geser-Khan, Berl., 1851, and B. JUlgin the Transaciumt
oftbe WiirzbnrgerPhlloI.Versam. ofl868, pp. 58*5^., Leips., 186^); and tbe tales
about Ardshi Bordski (Russian version by Galsang Gomooyew, Petersb., 1858 ;
text and German trans, by B. Jtllg, Innsbr., 1867, 1868). A favourite book Is^
the tales of Siddhi-kOr based on the Sanskrit Vetdla panckavini:a(i (Russiaa
trans, by GaLjang Gomboyew, Petersb., 1865 ; nine of the tales in MongoUari
and German by B. Jiilg, Innsbr., 1868). The fuller collection of these tales In
Kalmuk first became Itnown by the German trans, of B. Bergmann in vol. L
of his Nomadiscr.e Strei/ereun unter d. Kalmiiken (4 vols., Riga, 1S04, 1805) :
an autographed edition in the vulgar dialect was published by C. Golstunskyi
(Petersb., 1864 ; text and German trans, with glossary by B. Julg, Leips., 1865).
A poetic heroic story is the Djangariad, extracts from which were given by
Bergmann(op. ci(., iv. 181 sqq.); a complete Russian version by A. Bobrownikow
(Petersb., 1854); a German version by F. v. Erdmann in Z.D.M.G., 1857 (Kalmuk
text by Golstunskyi, Petersb,, 1864). A similar poem is the history of Ubaslu
Khuntaidshl and his war with the Oirad, Kalmuk text and Russian trans, by
■ G. Gomboyew in hii Altan tobtchi as above, and text alone autographed by
Golstunskyi (Petersb , 1864). Some books of religion for the Christian Buriat»
(transcribed in Russian characters) represent the Buriatlc dialect The Russian
and English Bible Societies have given us a translation of the whole Btble. L
J. Schmidt translated the Gospels and the Acts into Mongolian and Kalmnk.
for the Russian Bible Society (8 vols., Petersb., 1819-1821X— a masterly work.
The English missionaries, E. Stallybrass and W. Swan, and afterwards R. Tuille,
translated the whole Old Testament into Mongolian (1836-1840). This work waa
printed at a mission press erected at great cost for the purpose near Saelenginek,
beyond Lake Baikal in Siberia. In 1846 the New TesUment by the same haads
appeared at London.
The richest collections of Mongolian and Kalmuk printed books and MSS.
are in the Asiatic museum of the Petersburg Academy, and In the libmrte* rf
Kasan and Irkutsk ; there is also agood collection in the royal library at Dres-
den. Consult in general, besides the already-cited works of Bergmann and Po-
idnyeyew, P. 8. Pallaa, Samnlwtgen historisehtr Nachrichten ii. d. Mongoltxhtm
Volktrseha/tf'i (2 vols., Petersb., 1776-1801)-. I. J. Schmidt, Forschungtn in C«i)i«(#
der<cren . . . Bildun^gachichtedtrVolker Mitttlasitns.voTZ. d. MongaUn untt
Tibtter (Petersb. and Leips., 1824) ; B. J'Jlg, " On the Present SUte of Mongolian
Researohes," Journ. JL At. Soc., xiv. (1882), pp. 42-65. (B. J.)
MONGOOS, or >/7Naoo3. See Ichneumon.
MONITION, in the practice of the English ecclesiastical
courts, ia an order requiring or admonishing the person
complained of to do something specified in the monition,
** under pain of the law and penalty thereof." It is the
lightest form of ecclesiastical censure, but disobedience to
it, after it has been duly and regularly served, entails the
penalties of contempt of court. See Phillimore, EccUsi-
astical Law (London, 1873).
MONK, Geoege (1608-1669), duke of Albemarle, the
second son of Sir Thomas Monk, a gentleman of good
family but in embarrassed circumstances, was born at
Potheridge, near Torrington in Devonshire, on 6th Decem-
ber 1608. An exploit which brought him within the
reach of the law compelled him to begin his career as a
soldier of fortune at the age of seventeen. He acted
upder Sir R. Grenville as a volunteer in the expedition to
Cadiz, and the next year did notable service at the I&la cf
Rh6.
In 1629 Monk went to the Low Countries, the training
ground for military men, where in Oxford's and in Gorings
regiments he obtained a high reputation for courage and
for a thorough knowledge of his trade. In 1638 he
threw up his commission in consequence of a quarrel "with
the Dutch civil authorities, came to England, and obtained
the lieutenant-colonelcy of Newport's regiment during the
operations on the Scottish border. Here he showed his
skill and coolness in the dispositions by which he saved
the English artillery at Newborn, though himself destitute
of ammunition ; and in the councils of war he confidently
voted with Strafford for fighting, and against retreat or
composition. One of Monk's biographers relates that he
now thought of joining the adventurers who proposed to
colonize Madagascar. The Irish rebellion, however, offered
752
MONK
more congenial employment, and in February 1641 he
landed at Dublin as colonel of Lord Leicester's regiment.
Here be greatly increased his reputation. Under the most
difficult circumstances he was ever cool, patient, vigorous.
A rigid disciplinarian, he was always attentive to the wants
of his men, and completely won their confidence and affec-
tion. Ail the qualities for which he was noted through
life, the calculating selfishness which kept him ever on
the winning side and by which he accomplished hh great
historic success, the imperturbable temper aud impene-
trable secrecy, were fully displayed in this employment.
He had but one interest, that of George Monk ; and to
secure that interest he laboured, while retaining his free-
dom from party ties, to make himself indispensable aa a
soldier. The governorship of Dublin was vacant, aud Monk
was appointed by Leicester. But Charles L overruled the
appointment in favour of Lord Lambert, and Monk, with
great shrewdness, gave up his claims. Ormond, however,
who viewed him with suspicion as one of the two officers
who refused the oath to support the royal cause in Eng-
land, sent him under guard to Bristol. He now deemed
it safest to affect EoyaJist views. His value caused him
to be received at once into Charles's confidence ; he was
appointed major-general of the Irish brigade, and served
under Byron at the siege of Nantwich. Here he was
taken prisoner by Fairfax, on 25th January 1644, in one
of the most sldlful operations of the war. After a short
captivity in HuU he was placed in the Tower, where he
remained for three years (during which his father died),
beguiling his imprisonment by writing his Observations
on Militari/ and Political Affairs.
So long as the war lasted Monk could not be released.
Charles, however, became a prisoner; the troubles in
Ireland made the parliament anxious to secure Monk's
services, and he was told that if he would take the Cove-
nant he might have an important command. With some
show of hesitation the terms were accepted, and, after a
service of two months in Lord Lisle's abortive expedition.
Monk was placed in command of the British forces in the
north of Ireland. Compelled in 1649 to conclude a pacifi-
cation with the rebel O'Neill, he returned to England after
the king's execution. In the same year he succeeded, by
his elder brother's death, to the family estate. His idleness
lasted but * short while. CromweU gave him a regiment
and the command of the ordnance in the Scotch war of
1650, and after the battle of Dunbar, in which he led the
attack, he was left with 6000 men to subdue the country,
which, after taking Edinburgh, Tantallon, and Stirling
castles, he did most completely in a few weeks. In 1651
he was seized with fever, but recovered at Bath, and in
the same year was appointed on the commission for pro-
moting the Union. In 1653, with Admiral Dean, he
commanded the British fleet against the Dutch, and on
2d and 3d June and 29th July fought two of the most
sanguinary naval battles on record, in which both his
colleague and Van Tromp were slain. A peace on very
humiliating terms to the Dutch was concluded, but policy
shortly led Cromwell to allow milder conditions, — a conces-
sion against which Monk strongly remonstrated. On his
return he married his mistress, Anne Clarges, a woman of
the lowest extraction, " ever a plain homely dowdy," says
Pepys, who, like other writers who mention her, is usually
stOl less complimentary. Monlc was now sent to quell the
revolt headed by Middlcton in Scotland, and, when tliis
service was over, settled down to a steady government of
the country for the next five years. For fanaticism in any
shape be hf!-l no syr.-jx'.t'iy, and he set himself to diminish
;tho indueAce of the Presbyterian clergy — Cromwell's chief
(.;,;^oncnt3, — taking from them the power of excommuni-
cation and their geaeral assemblies, but allowing them to
retain their prorbytories. Equal repression was exercised
against the nobility and gentry. The timely discovery of a
plot fomented by Overton for killing Monlc on New Year's
Day gave him an excuse for thoroughly purging hia army
of all Anabaptists, Fifth Monarchy men, and other danger-
ous enthusiasts. It is doubtful whether at this time Monk
had proposed to himself the restoration of the king. He
probably had it always in his mind as a possibility, but he
woWd run no risks. His very reticence, however, caused
alarm on one side and hope on the other. In 1655 .be
received a letter from Charles II., a copy of which hu at
once sent to Cromwell, wliom, however, we find wrjliug tc
him in 1657 in the following terms: "There bo that tell
me that there is a certain cunning fellow in Scotland callo
George Monk, who is said to lye in wait there to introduc.
Charles Stuart ; I pray you, use your diligence to appre
hend him, and send him up to me."
During the confusion which followed Cromwell's death
Monk remained silent and watchful at Edinburgh, careful
only to secure his hold on his troops. In July 1659
direct and tempting proposals were again made to him
by the king. His brother Nicholas, a clergyman, was em-
ployed by Sir J. Grenvil to bring to him the substance of
Charles's letter. No bribe, however, could induce him to
act one moment before the right time. He bade his
brother go back to his books, and refused to entertain any
proposal. But when Booth rose in Cheshire for the king,
so tempting did the opportunity seem that he was on
the point of joining forces with him ; and a letter was
written to the Rump parliament threatening force if it
did not at once fill up its numbers. His habitual caution,
however, induced him to wait until the next post from
England, and the next post brought news Of- Booth's
defeat. On 17 th October he heard of Lambert's coup
d'etat. From that moment his plan of action seems to
have been settled. In most vehement language he dis-
carded the idea of restoring Charles, and, with admirAble
perception of the state of English feeling, took for his
principles that in aU cases the army inust obey the civil
government, and that the civil government must be
parliamentary. At present the Rump was crushed by the
military party ; the first thing, therefore, to be done was to
free it. His army vmderwent a second purging of dis-
affection, and he then issued a declaration embodying the
principles mentioned above, and wrote to Lenthall the
speaker, and to ■ the military party to the same effect.
In a treaty with the Committee of Safety his commissioaers,
who were to" treat only on the basis of the restoration of
parliament, were outwitted. Monk at once refused to
accept the terms proposed, and marched to Berwick, having
received an offer from Fairfax of assistance if he would
promise that the secluded members should be restored.
Meanwhile Lambert had marched northwards to oppose
his advance.
Monk's action gave fresh heart to the adherents of the
parliament. The old council of state met, and named
him general of all the forces ; the fleet and the Irish
army, hitherto hostile, came round to his side, and so did
Whethara at Portsmouth. Monk now, in the depth of
winter, crossed the Tweed at Coldstream and marched hy
Morpeth to- Newcastle, receiving letters on his way from
the lord mayor and corporation of London urging him to
declare for a free parliament. On his approach Lambert's
army fell away from their general, and r •> obstacle re-
mained on tlie path to London. At York, tvhen urged by
Fairfax, he refused to declare for the king, and is said to
have caned an officer who affirmed that such was his
design. The pariisiraent now ordered him to come to
London. Fleetwood's army wliich occupied the city was,
however, a great obstacle ; and it was not until the parlia-
k
/m: O N — M O N
753
inent, in. accordance with his desire, had arranged for its
dispersion that he would enter with his troops. Even
now his intentions were strictly concealed; the spies set
upon him by the various anxious parties were baffled by
IhiB impenetrable reserve. He was careful to appear only
bthe servant of parliament, but when he was desired to
ke the oath of abjuration he skilfully evaded the request.
The city, always jealous of the Bump, now refused to pay
taxes except at the orders of a free parliament. Monk,
in consequence, was ordered to march his troops into the
city, take down the chains and posts, and unhinge the
gates. He obeyed these unpleasant orders to the letter on
10th February, thus permitting the hatred against the
Rump to rise to the height, while he showed how unwilling
an instrument of its will he was. On the 11th, however,
ho threw off the mask, and wrote to the Rump; peremp-
torily ordering them to admit the secluded members, and
to arrange for the dissolution of parliament by 6th May.
On 2l8t February he conducted the secluded members
to their seats. At the same time he refused to restore
the Lords, and issued an order disowning Charles Stuart
to all officers commandiug garrisons. Eveiy day brought
him fresh opportunities for tact or evasion. His partisans
urged him to take the protectorate himself; another party
pressed upon him to accomplish the restoration by the
army alone ; a body of his officers sent him a declaration
expressing their fears that his action would lead to the
restoration of monarchy ; the parliament tried to make
him their own by the offer of Hampton Court. His
trained habits of dissimulation and evo,sion, assisted now
and again by downright lying, carried him triumphsntly
through all these dangers, and at length the dissolution of
parliament on 17th March removed his greatest difficulties.
It was now that, with the utmost secrecy, he gave an
interview for the first time to the king's agent Grenvil,
and by him sent to Charles the conditions of his restoration,
afterwards embodied in the Declaration of Breda. For
himself at present he would accept nothing but a royal
coiomission as captain-general, which he carefully kept
to himself. All parties were anxious to gain the credit of
the now ceVtain restoration. The Presbyterians in parti-
cular, fearful of the king being restored without terms,
did their best to discredit Monk and to impose the old Isle
of Wight conditions ; but in vain. The new parliament was
elected, and the House of Lords restored ; an insurrection
by Lambert, who had- escaped from the Tower, was quelled
by Monk's prompt measures, and on the 25th of April he
received the solemn thanks of both Houses, and the title of
captain-general of the land forces. Even yet the farce
was kept up. Monk received with feigned surprise the
king's official letter from Grenvil, denied all knowledge
of its contents, and handed it over sealed to tlie council,
who decided to defer opening it imtil the meeting of
parliament on the Ist of May.
With the Restoration the historic interest of Monk's career
ceases. The rude soldier of fortune had played the game
with incomparable dexterity, and had won the stakes. He
was made gentleman of the bedchamber, knight of the
Garter, master of the horse, commander-in-chief, and duke of
Albemarle, and had a pension of £7000 a year allotted him.
His utmost desires were satisfied, and he made no attempt to
compete further in a society in which neither he nor his
vulgar wife could ever be at home, and which he heartily
despised. As long as the army existed of which he was
the idol, and of which the last service was to suppress
Vernier's revolt, he was a person not to be displeased.
But he entirely concurred in the measure for disbanding
it, and thenceforward his influence was small, though men's
eyes turned naturally to him in emergency. In the trial
•f the regicides he was on the side of moderation, and his
interposition saved Hazelrig's life ; but his action at tha
time of Argyll's trial will always be regarded as the most
dishonourable episode in his career. In 1664 he had'
charge of the admiralty when James was in conmiand o{
the fleet, and when in 1665 London was deserted on'
account of the plague. Monk, with all the readiness of a
man accustomed to obey without thinking of risk, remained
in charge of the government of the city. Once more, at
the end of this year, he was called upon to fight, having a
joint commission with Prince Rupert against the Dutch.'
The whole burden of the preparations fell upon him. On
23d April 1666 the admirals joined the fleet, and on the 1st
of June began a battle near Dunkirk which lasted four days,
followed by another on 23d July, in which Monk showed
all his old coolness and skill, and a reckless daring which
had seemed hitherto foreign to his character. His last
service was in 1667, w^hen the Dutch fleet sailed up the
Thames, and Monk, ill as he was, hastened to Chatham to
oppose their further progress. From that time he lived
much in privacy, and died of dropsy on the 3d of Deceuiber
1669.
Sec the Lives of Monk by Dr Gumblo, his chaplain (Loiidon, IfiTI) ,
and Dr Skinner (London, 1724), auj Guizot's Esstvj, which contani
all necessary information concerning his life up to the Restoration.
The numerous and amusing notices of him in the court of Charles
in Pepys's Diary should on no account be omitted. (0. A,)
MONKEY. See Ape.
MONMOUTH, a maritime county of England, is bounded P!«S? TX.
E. by Gloucester, N.E. by Hereford, N.W. by Brecknock,
W. and S.W. by Glamorgan, and S. by the Bristol Channel.
Its greatest length from north to south is about 35 miles,
and its greatest breadth about 28 miles. The ai'ea -is
368,399 acres, or about 572 square miles.
The surface of Monmouth is very varied, and m many
districts picturesque, especially along the valley of the
Wye, and between that river and the Usk. In the west
and north the hills rise to a considerable height, and this
mountain region encircles a finely undulating country.
The highest summits are Sugar Loaf (1954 feet), Blorenge
(1908), and Skyridd Vawr (1601). Along the shore on
both sides of the Usk are two extensive tracts of marsh
land, called the Caldicot and Wentllooge levels, stretching
from Cardiff to Portskewett, and protected from inunda-
tions by strong embankments.
The principal rivers are : the Wye, which forms the
eastern boimdary of the county with Gloucester, and falls
into the Severn ; the Monnow, which forms a portion of its
boundary mth Hereford, and falls into the Wye at the
to^vn of Monmouth ; the Usk, which rises in Brecknock,
and flows southward through the centre of the county to the
Bristol Channel ; the Ebbw, which rises in the north-west,
and enters the estuary of the Usk at Newport ; and the
Rumney, which rises in Brecknock, and, after forming the
boundary between Monmouth and Glamorgan, enters the
Bristol Channel a little to the east of Cardiff. Salmon
abound especially in the Wye and the Usk, and trout are
plentiful in all the streams. The Monmouthshire canal
extends from Newport to Pontypool, where it is joined by
the Brecknockshire canal, which enters the county near
Abergavenny. ■ The Crumlin canal also joins it a little
north of Newport.
Ocology and Minerals. — Tlie geological formation is principally f
Old Red Sandstone and Carboniferous, — the Old Red forming tha
larger and eastern half of the count}', from a line drawn between
Abergavenny and Newport, and varying in thickness from betweea
8000 «nd 10,000 feet iin the north to-about 4000 feet in the south.
In the centre of the county adjoining the Usk there is an outcrop
of Silurian rocks, extending to a distance of about 8 miles north
and south and 4 miles east and west, ivith a thickness of 1500 feet
Towards the east the Old Sandstone rocks dip beneath the Moun-
tain Limestone, which enters the county from the Forest of Deau
coal-field, and gives its peculiar character to the fine scenery along
the banks of the Wye. The formation varies in thickness from-
16—27
754
IZ lu r^ ,Tho Carbomferous rocka cormectod ,vith the great
coal-field of South TV ales, which occupy the western haU- oftho
couuty, mclude-(l) the Coal-measures, consisting of "hales and
.rons tones, sandstones and coal-beds, of which fhe.e are about
rt;^F;^'«%ni' rZ^K^X^ '"*■ 'W^><-total thickness of the
stiata 11,650 feet; (2) Millstone Grit, thickness 330 feet- (3)
Juuu leet , (4) Old Red Sandstone, thickness 600 feet : and (5)
Devomau beds, consisting of red and brown sandstone, marirtc
thickness about 6000 feet. The coal-field of Monmouth has an area
of about 90,000 acres. The beds are very rich and e«ily 4ou'ht
the most common way of reaching them being by exca/attl° T>aa-
Tfe'numtVof™ V^' ^^^ '°'"^?'' "^ ''5' P"P«°dicular sliafts.
ine number of collieries m operat on in 1881 was I^i and tl,.
Tiianhty of coal obtained 5,412:840 tons. The ironstone of M n
mout occurs bo h in beds and in large detached masses, the yiehi
stone T^° ^ *°- ^° ^' ""*• ^^' "^ '"" "^« ™"™o'' '^'ar ron-
stone. The iron industry was prosecuted successfully at Poutv-
pool m the 16th century by a family of the name of (i„nt wl o
were succeeded by the Hanbuiys. In 1740 Monmouth contained
anZn'v ™'y '^".f""?"^. «l'i--'l' >nade together about 900 to ^
annually ; but aunng the piesent century they have increased with
grea rapidity. In 1S81 the number of furnaces built was 5^
f.J'ifJl "^ '"'%"' operation ; the amount of pig-iron made was
of kn,I°"',- ^^ '^°'^ ^? ''^"''"^ ''^''^y '" "'» neighbourhood
i'ertlt^Tv°dfii'-'^rr''P^ the vaUeys running in the direction of
Merthyr-Tydfil in Glamorganshire. The following were the Mon
Ebbl vT'v-'^ '" ^^i\ = ^^"^y^^^'^' Pontypool,°Pontnewynydd;
Ebbw \ale. Victom, Blaenavon, Cwmbran. Nantyglo. Oakfields
Blaina. Rhymney and Tredegar. In aU, there w-ei^®S8 puddling
furnaces and42 rolling mills in operation. 'The tinplate man'^fachirt
B extensively earned on, the number of mills in the Monmouth and
Gloucester ctotnctn 1831 being 95, the majority of which are"n
Monmouth. Fireclay is extensively dug ; 57. 680 tons we'e obtained
Soil and JorimUure.—A]ong the sea.^horo the soil is deen and
oamy and admirably suited for the gi-owth of t^e s. Th^most
teni'lf rt ^'i^'^fti^S °" K^d Sanllstone, especially along the
t>e^„/ "?■ "■'''" ''^'^^ ^ '"^'^^ »' » ^-^y fiDi= quality In
iMeTcult;Z^n°''Sf "=g.'°f .th-re is very little land that b cap
attentLr/ /?' *''° •""' ^""^ generally thin and peaty. Mo e
attention is naid to grazing than to the i-aising of crops. There are
a considenbie number of dairy-farms, but sheep-far£in/fs much
Eore largelj followed. Of the 5241 holdings exisring inlssO-tlie
fetest year in regard to which there is information_3661 were unde?
60 =«=reslooi between 50 and 300 acres, and only 59 above 300
l4^nr, ""''^°°,*° thoagricultural returns for 18S2 th™ were
cnltivatior^'oT M^I-fT-S'' '"°"*"'^ "' ""^ ""'' -^^. "°d-
cultivation. Of th.^ ,6,137 ac«s were _permanent pasture, and
M O N M OUT H
IfiT^i "onfff^sfs. Of the 35.038 acres under corn croiM
16,151 were under wheat, 8596 under barley, and 8711 under oat?
UDieCt 7486 ncvp<z anA n..,fnf.. — 1_ 1-T.T-. n..
14,729 rotation grasses.
16,151 were under wheat, „^i,u uuuer oaney, ana bJV
Turnips occupied 7486 acres, and potatoes only 1777 The area
under woods was 29.856. and under irehards 3921. The total num
for alt'lf '", '''' ^''' ''•'^' ■■ «f "'"^I' «'<= ■^"'nl^eV us d solrfy
for agncultura purposes was 6449. Of the 44,168 cattle 16 500
and pi^ 17,6Jl. According to the latest return there were 7811
S2 r'^oTtr'"" 2»S'f,l«"^=. ^"th a gross annual enti of
1 ,e,; 17 « the owners, 4970, or 63 per cent., possessed less than
L^„ ' V possessed between 1000 and 2000 acres and 15 befw«n
^n'^oii T Lady Llanover. 6312 ; the eMcutors of C. H. Lci^h
10,211 ; Lord Tredegar, 25,229; and the duko of Beaufort 27 299 '
iJni/imy,. -The South Wales Railway passes alon^ the coast
and many branch Hnft cross the count/in various d"?ect on the
majonty of them being connected eithir with the Gieat ^e^teru
Railway or with the London and North- Western
yidminwtralion and Population.-Honmouth comprises six lun-
^8 427t In i^H^''^' 'T"^'^' of Monmouth (611lfand New trt
(38,427). In addition to these two borouchs there iin l\rt,.L,, '
Banitary districts, viz.. Abergavenny (6^41 ) Abersyrha n3 •oA"
AbertUlery 0003), Blaenavon (9451) Caerleon nOOT? rJ ' '
(359-1), Christchurch (3114), Ebbw- Tab (14 700^ 'u^if'"'''
(4177), Panteg (3321), Pontj-pool (5244) Rhvmnev'«6f"rP^
(5540), Tredegar (18.771), i/sk (l470).'' W^Hl e SionTf
Abergavenny, Caerloon, Chepstow, Pontypool, and Usk. these tow"s
are all of modem growth, and owe their rise chiefly to the i^-on
Sit '■■i~"'""v'"'^-'"' '"='"S P»"ly dependeift on hat of
tiiiplate. ho county returns tivo members to narlimwnt • LJ
of 46,033, constitute the Monmouth disti-ict of'boWhs wMch
returns one member. The county h.as one court of quarter sessions
«nd 13 dm.Ied into twelve petty sessional divisions. It U witl",;
the diocese of Llandair. and contains 147 civil parishes- town^hin,
or places. The population, which in ISOl was 45.568 hkd ii^re.T. 1
Khom 108,262 were males, and 103,005 females). '=''.':»' (of
^^^'sTie^rm^-'^foTthTt'^^^^^^^
7heL ^ In the QH ^Pfrf/u S°™™°>'="t distinct from either of
Sged^t^nT^ 'f^^^h^^^^r.^zr^
Portskew^? r' It'tt n'"'' -'-W-l>'d a palaceat p",h-£cred
Shtom *'^-'f"'^ ^*'^'' *'y colquer^ed^'i't™ ':*w^f.'h
&rh^^^h:t.:-.J?4Sc^
of?yft^To?d'ro'?Te^m''r"?K''''"'''"''""'-°^'«°P»-^^^^^
frwentvfivi Tl marches there are remains of no less than
twenty-five. The more interesting and important are • Caldicot f>°
th^Tifh I ■ ^"^an fortress extant, buUt by Fitz Osboni hi
|:^™:K2k::;vi!^:?--^^fe|^S
vahon, and contains examples of se,eral styles of Sdrite^ctoe
Charles I. resided m it after the battle of Naseby. In 1646 it wa.
delivered up to the parliament. "
fifttL'i°i ^'fo^.a^oi? there were in Monmouth two hospitals and
fifteen other religious houses ; but of these there are now ^Bortant
occupies a position of great beauty on the Wye. The b^Udin^
whicl, IS Early English to Decorated, is almost entire with t^e
exception of the r<^f, and may be ranked as among the fines of the
TZTh ™'"%'k ^"S'^""^- .°f "'^ ^>"^''". "-"^^ chiefly worthy
of mention are Abergavenny, belonging to a Benedictine priory and
containing a number of old tombs ; Chepstow, partly NoS aud
possessing a nchly-nioulded doorway; S^Vooloschui4! Newport
also Norman ; the Norman church of St Thomas, Monmouth ; ChrUt
Church prmcipally N orman ; Matherne, Early English, with k tablet
dic?hilt^l;rv!"^ of Gwenf; and Usk. formeriy attached to a Bene'
SIoNMOOTH (Welsh Jfmzoy), a parliamentary and muni-
cipal borough of England, and the county to\vn of Mon
mouthshire, is pictiu-esquely situated at the confluence of
the Wye and Monnow, in a valley almost siu-rounded by
hills, 18 miles south of Hereford, and 12S west of Loudon
By means of the Wye it has water communication with
Bristol and with Hereford, but the former trade by barges
has now ceased. Portions of the old walls and of the four
gates still remain; but there are only insignificant ruins of
the old castle in which Henr)- V. was born, aud which was
originally a Saxon fortress. After the Norman Conquest
It was placed in the hands of William Fitz Osborn, whosa
descendant, John lord of Moumouth, rebuilt it on a more
extensive sca^e. Sub.seque„tly it came into the possession
of John of Gamit, and thus became attached to the house
of Lancaster. In 1C46 it was taken by the parliamentary
M 0 N M O U T. Ja
75b
forces. Besides the cliurches — the new church of St Mary,
completed in 1882, and the' church of St Thomas, an Old
Norman structure — the principal public buildings are the
market -house, the town -hall, and Jones's free grammar
school in the Tudor style, which dates from 1614. The
manufactures of the town are unimportant. The fine
scenery of the Wye attracts a large number of tourists.
Monmonth was one of the strongholds of the Sa:;on8 ; and under
the name of Blestium formed one of the stations of the Romans.
It was incorporated by Edward VI., and received additional privileges
from Queen Mary^ James I., and Charles II. It has sent members
to parliament since the 27th of Henry VIII., and, along with New-
port and Usk, forms the Monmouth district of boroughs. The area
of the municipal and parliamentary borough is 4983 acres, with a
population in 1871 of 6879, and in 1881 of 6111.
MONMOUTH, a small manufacturing city of the
United States, in Warren county, Illinois, 180 miles south-
west of Chicago by the main line of the Chicago, Burling-
ton, and Quincy Eailroad, and 182 miles north of St
Louis, by the St Louis division of the same railway. The
Iowa Central Eailway passes through the city. An opera-
house and Monmouth College are among the principal
buildings. The population increased from 4662 in 1870
to 5000 in 1880. The city charter dates from 1852.
MONMOUTH, James, Ditke of (1649-1685), was the
son of Lucy Walters, "a brown, beautiful, bold, but insipid
creature," who became the mistress of Charles II. during
his exile at the Hague. He was born at Rotterdam on
9th AprU 1649. That Charles was lus father is more
than doubtful, for Lucy Walters had previously lived with
Robert Sidney, brother of Algernon, and the boy resem-
bled him very closely. Charles, however, always recog-
nized him as his son, and lavished on him an almost doting
affection. Until the Restoration he was placed under the
care, first of Lord Crofts, and then of the queen-dowager,
receiving bis education to the age of nine from Roman
Catholics, but thenceforward from Protestant tutors. In
July 1662 he was sent for by Charles, and at thirteen was
placed under the protection of Lady Castlemaine and in the
full tide of the worst influences of the court. No formal
acknowledgment of his relation to the king was made
until his betrothal to Anne Scott, daughter of the earl of
Buccleuch, and the wealthiest heiress of Scotland, whom
he married in 1665. During 1663 he was made duke of
Orkney, duke of Monmouth, and knight of the Garter,
and received honorary degrees at both universities. At
court he was treated as a prince of the blood. In 1665
he .'served with credit under the duke of York in the san-
guinary naval battle off Lowestoft. A captaincy in the
Life Guards was given him, and in 1670, on the death of
Monk, he was made captain-general of the king's forces.
Offices of wealth also were showered upon him, and he was
admitted to the privy council. In 1670 Monmouth was
with the court at Dover, and it is affirmed by Eeresby
that the mysterious death of Charles's sister, the duchess
of Orleans, was due to her husband's revenge on the dis-
covery of her intrigue with the duke. It is certain, from
an entry by Pepys, that as early as 1^66 he had estab-
lished a character for vice and profligacy. He was the
direct author of the attack in December 1670 on Sir John
Coventry, and only a few months later received the royal
pardon for his share in the wanton murder of a street
watchman. De Gramont, in his vivid sketch of Mon-
mouthj after describing the beauty and bodily prowess for
which he was celebrated, notices the fatal emptiness and
poverty of his mind: "Tous les avantages du corps par-
loient pour lui ; mais son esprit ne disait pas nn petit mot
pn sa faveur. II n'avait de sentunens que ce qu'on lui en
inspirait."
Hitherto Monmouth had been but the spoiled child of
a wicked court. Now, however, by no act or will of his 1
own, he began to be a person politically important. As
early as 1662 the king's excessive fondness for him had
caused anxiety. Even then the fear of a "difference"
between Monmouth and James, duke of York, exercised
men's minds ; and every caress or promotion kept the fear
ali ve. Who could tell but that, in default of legitimate issue
from his queen, Charles might declare Monmouth himself his
lawful son 1 A civil war would be the certain consequence.
Soon after 1670 the matter took a more serious aspect.
The anti-popery spirit was tapidly becoming a frenzy,
and the succession of James a probability and a terror.
Charles was urged to legitimize Monmouth by a declara-
tion of his marriage with Lucy Walters. He returned
answer that, much as he loved the duke, he would rather
see him hanged at Tyburn than own him for his legitiJ
mate son. Every attempt, however, was henceforth made;!
especially by Shjiftesbury, to accustom people to this idea.'
He was taught to regard himself as the representative of
the Protestant interest, and his position was emphasized by|
James's,second marriage with the Roman Catholic princess
Mary of Modena. From this time his popular title was " the
Protestant duke." Charles was induced to confer many
prominent employments upon bim, The influence of James,
however, was strong enough to prevent his obtaining the
lord-lieutenancy of Ireland ; but he received the command
of the 6000 troops who assisted the French in the second
Dutch war, and, though without any claims to generalship,'
behaved with courage in the field. In 1674 he was made
"commander-in-chief;" and, in connexion with this, another
unsuccessful attempt, graphically described in Clarke's
Life of James, .was made to gain from Charles a tacit
admission of his legitimacy. At Shaftesbury's instance
he was placed in command of the army employed in 1676
against the Scottish Covenanters, and was present at Both-
well Bridge (22d June 1679). He was also, at the king's
request, elected chancellor of the university of Cambridge.
In 1678, when Charles was driven into war vrith Louis,
Monmouth took the command of the English contingent,
and again gained credit for personal courage at the battle
of St Denis. On his return to London England was in
the throes of the popish terror. The idea of securing the
Protestant succession by legitimizing Monmouth again took
shape and was eagerly pressed on by Shaftesbury ; at the
time it seemed possible that success would wait oB the
audacity.
The Pensionary parliament was dissolved in January
1678-79, and was succeeded by one still more determined
in its anti-popery spirit. To avoid the storm, and to save,
if possible, his brother's interests, Charles instructed him
to leave the country. James retired to Brussels, the king
having previously signed a declaration that he "never
was married, nor gave contract to any woman whatsoever
but to my wife Queen Catheriiie." In spite of this, Mon-
mouth might naturally now nourish ambitious views.
EQs rival was off the stage; Shaftesbury, his chief supporter,
was president of the remodelled privy council ; and he
himself was the favourite of the city. In the summer of
1679 the. king suddenly fell iU, and the dangers of a dis-
puted succession became terrilily apparent. The party
opposed to Monmouth, or rather to Shaftesbury, easily
prevailed upon Charles to consent to his brother's tem-
porary return, 'When, after the king's recovery, James
went back to Brussels, he received a promise that Moit
mouth too should be removed from favour and ordered
to leave the country. Accordingly, in September 1679,
the latter repaired to Utrecht, while shortly afterwards
James's friends so far gained ground as to obtain for In"™
permission to reside at Edinburgh in.?tead of at Bnissels.
Within two months of his arrival at Utrecht, Monmouth
secretly retm-ned to Ensland. aTrivLig ia London on 27th
756
MONMOUTH
November. iSliaftesbury bad assiduously Kept aave tbe
anti-popery agitation, and Monmouth, as the champion of
Protestantism, was received with every sign of popular
delight. The king appeared to bo greatly incensed,
deprived him of all his offices, and ordered him to leave
the kingdom at once. This he refused to do, and the only
notice taken of the disobedience was that Charles forbade
him to appear at court.
It was at this time that the Appeal from the Country to
the City, written by Ferguson, was published, in which
the legitimacy was tacitly given up, and in which it was
urged that " he that hath the worst title will make the
best king." Now it was too that the exclusionists, who,
in the absence of parliament, were deprived of their best
basis for agitation, developed the system of petitioning.
So- promptly and successfiilly was this answered by the
" abhorrers " that Charles, feeling the ground safer under
him, recalled James to London, — a step immediately fol-
lowed by the resignation of the chief Whigs in the councU.
Once more, however, a desperate attempt was made, by
the fable of the "black box," to establish Monmouth's
claims ; and once more these claims were met by Charles's
public declarations in the Gazette that he had never been
married but to the queen. Still acting under Shaftesbury's
advice, Monmouth now went upon the first of his progresses
in the west of England, visiting the chief members of the
country party, and gaining by his open and engaging
manner much popularity among tbe people. • In August
1680 James returned to Edinbiu-gh, his right to the suc-
cession being again formally acknowledged by Charles.
Monmouth at once threw himself more vehemently than
ever into the plans of the exclusionists. He sp(»ke and
voted for exclusion in the House of Lords, and used lan-
guage not likely to be forgotten by James when an oppor-
tunity should come for resenting it. He was ostenta-
tiously feasted by the city, the stronghold of Shaftesbury's
influence ; and it was observed as he drove to dinner that
the mark of illegitimacy had been removed from the arms
on his coach.
The year 1G81 seemed likely to witness another civil
war. 'The parliament finished a session of hysterical pas-
sion by passing a series of resolutions of extreme violence,
of which one was that Monmouth should be restored to
all his offices and commands; and when Charles summoned
a fresh parliament to meet at Oxford the leaders of the
exclusionists went thither with troops of armed men.
Not until the dissolution of this last parliament on
27th March 1681 did the weakness of Monmouth's cause
appear. In a moment the ground was cut from under
the feet of his supporters ; their basis for agitation was
gone ; pamphlets and broadsheets could ill supply the
place of a determined and unscrupulous majority of the
House of Commons. The deep-seated respect for legitimate
descent asserted itself, and a great reaction took place.
In November Dryden published Absalom and Achitophel.
Shaftesbury was attacked, but was saved for the time by a
f avouring j ury. Monmouth himself did not escape insult
in the street and from the pulpit. He thought it wise to
try to make his peace with the king, but he did so in
terms which incensed Charles the more. He was forbidden
to hold communication with the court ; and, when he went
in September 1682 on a second progress through the
western and north-western counties, his proceedings were
narrowly watched, and he was at length arrested at Staf-
ford. Severity and extreme lenity were strangely mingled
in the treatment he received. He was released on bail,
and in February 1683, after the flight and death of Shaftes-
biuy, he openly broke the implied conditions of his bail
by paying a third visit to Chichester with Lord Grey and
other? on pretence of a hunting expedition.
It is probable that Monmouth never went so far as W
think of armed rebellion ; but there is little doubt that ha
had talked over schemes likely to lead to this, and that
Shaftesbury had gone further still. The Rye House plot
gave an excuse for arresting the Whig leaders ; Eussell
and Sidney were judicially murdered ; Monmouth retired
to Toddington in Bedfordshire, and was left untouched.
Court intrigue favouring him, he succeeded, by the betrayal
of his comrades and by two submissive letters, in reconciling
himself with the help of Halifax both to the king and to
James, though he had the humiliation of seeing his con-
fessions aL-d declarations of penitence published at length
in the Ga,:ette. His character for pettishness and folly
was now amply illustrated. He denied that he had given
evidence ; he then wrote a recantation of the denial. He
managed by importunity to get from the king the paper
of recantation ; and lastly, by the advice of his wife, he
ofi"ered again to sign the paper which he had withdrawn.
Charles heartily despised him, and yet appears to have
retained affection for him. His partial return to favour
raised the hopes of his partisans ; to check these, Algernon
Sidney wiis executed. Monmouth was now subpoenaed to
give evidence at the trial of young Hampden. To escape
from the difficulties thus opened before him he fled to
Holland, probably with Charles's connivance, and though
he once more, in November 1684, visited England, it is
doubtful whether he ever again saw the king. From that
time till the king's death he lived with Henrietta Went-
worth, his mistress, in Holland and at Brussels.
The quiet accession of James II. soon brought Monmouth
to the crisis of his fate. Though at first desirous of retire-
ment, his character was too weak to withstand the urgency
of more determined men. Within two months of Charles's
death he had yielded to the impetuosity of Argyll and
others of the exiles, and to vague invitations from England.
It is curious, as showing the light in which his claims
were viewed by his fellow-conspirators, that one of the
terms of the compact between them was that, though
Monmouth should lead the expedition, he should not assume
the title of king without their consent, and shoidd, it the
rebellion were successful, resign it and accept whatever
rank the nation might ofl'er. No" as always, he was but
a puppet in other men's hands.
On the 2d of May Argyll sailed witn tnree snips to raiet
the west of Scotland ; and three weeks later, with a following
of only eighty-two persons, of whom Lord Grey, Fletcher
of Saltoun, Wade, and Ferguson, the author of the Appeal
from the Country to tlie City, were the chief, Monmouth him-
self set out for the west of England, where, as the strong-
hold of Protestant dissent and as the scene of his former pro-
gresses, he could alone hope for immediate support. Even
here, however, there was no movement ; and wlien on 11th
June Monmouth's three ships, having eluded the royal fleet,
arrived ofl' Lyme Kcgis, he landed amid the curiosity rather
than the sympathy of the inhabitants. In the market-place
his "declaration," drawn up by Ferguson, was read aloud.
In this document James was painted in the blacltcst colours.
Not only was he declared to be the murderer c{ Essex, but
he was directly charged with having poisoned Charles to
obtain his crown. Monmouth soon collected an undisci-
plined body of some 1500 men, with whom he seized
Axminster, and entered Taunton. Meanwhile the parlia-
ment had declared it treason to assert Monmouth's legiti-
macy, or his title to the crown ; a reward of £5000 was
oflfered for him dead or alive, and an act of attainder was
passed in unusual haste. Troops had been hurriedly sent
to meet him, and when he reached Bridgwater Albemarle
was already in his rear. From Bridgwater tbe army
marched through Glastonbury to attack Bristol into whicl*
Lord Feversham. had hastily thrown a regiment of foot.
M O N — M O K
757
rgnards. The attempt, however, miscarried; and, after
sammonlng Bath in vain, Monmouth, with a disordered
force, began hia retrograde march through Philips-Norton
and Frome, continually harassed by Feversham's soldiers.
At the latter place he heard of Argyll's total rout in the
western Highlands. He was now anxious to give up the
enterprise, but was overruled by Grey, Wade, and others.
On the 3d of July he reached Bridgwater again, with an
army little better than a rabble, living at free quarters
and behaving with reckless violence. On Sunday the 5th
Feversham entered Sedgemoor in pursuit ; Monmouth the
same night attempted a surprise, but his troops were hope-
lessly routed. He himself, with Grey and a few others,
fled over the Mendip Hills to the New Forest, hoping to
reach the coast and escape by sea. The whole country,
however, was on the alert, and at midnight on the 8th,
within a month of their landing, James heard that the
revolt, desperate from the first, was over, and that his rival
had been captured close to Eingwood, in Hampshire.
The poor strain in Monmouth's character was now
shown. On the day of his capture he wrote to James in
terms of the most unmanly contrition, ascribing his wrong-
doings to the action of others, and imploring an interview.
On the 13th th& prisoners reached the Tower, and on
the next day Monmouth was allowed to see James. The
accounts of this interview are difficult to reconcile in some
points, but all agree that Monmouth's behaviour was un-
manly in the extreme. No mercy was shown him, nor did
he in the least deserve mercy ; he had wantonly attacked
the peace of the country, and had cruelly libelled James.
The king had not, even in his own mind, any family tie to
restrain him from exercising just severity, for he had never
believed Monmouth to be the son of any one but Robert
Sidney. Two painful interviews followed with the wife
for whom he bore no love, and who for him could feel no
respect ; another imploring letter was sent to the king, and
abject protestations and beseechings were made to all whom
he saw. He offered, as the last hope, to become a Roman
Catholic, and this might possibly have proved successful,
but the priests sent by James to ascertain the sincerity of
his " conversion " declared that he cared only for his life
and not for his soul.
He met his death on the scaffold with calmness and
dignity. In the paper which he left signed, and to which
ho referred in answer to the questions wherewith the
busy bishops plied him, he expressed his sorrow for having
assumed the royal style, and at the last moment confessed
that Charles had denied to him privately, as he had publicly,
that he was evoi' married to Lucy AValters. He died at the
age of thirty-six, on the 15th of July 1685. " Thus ended,"
says Evelyn, "this quondam duke, darling of his father
and the ladies, being extremely handsome and adroit ; an
excellent souldier and dancer, a favourite of the people, of
an easy nature, debauched by lusts, seduced by crafty
knaves, who would have set him up only to make a pro-
perty, and took the opportunity of the king being of
another religion to gather a party of discontented men.
He failed and perished."
Ai'.thoi-itics for Monmouth's career are, besides the known modem
liistories, Roberts's Life (1844), Evelyn's and Pepys's Diaries, Old-
mixon's History (1724), James II. 's Memoirs, Clarice's Life of Jama,
Kercsby's Memoirs, Sidney's Diasi^ (1843), Scott's notes to Absalom
a^ul Adiitopltel, and The Heroic Life, ic. (1633). For the rebellion.
Lord Grey's Secret History should be consulted. (0. A.)
itONMOUTH, Geoffrey of. See Geoffeey of Mon-
j:(.>rxH.
ilONOPHYSlTES. See Eutyches and Jacobite
Chcrch.
MONOPOLI, a city of Italy, in the province of Bari, is
situated on the coast of the Adriatic, 25 miles by rail
south-east of Bari. It u a bishop's see, is surrounded by
ancient walls, and possesses a castle buQt by Charles T. in
1552, a cathedral, and a hospital dating from 1368. The
harboxir is neither large nor well protected, but a certain
amount of trade is carried on in the export of local pro-
ducts. The population was about 12,000 in the 17th
century; 12,377 in 1861; and 13,000 in 1871, that of
the commune being 20,918. Monopoli probably grew up
after the destruction of Egnatia (5th century), the ruins
of which lie a few miles to the south.
MONOPOLY (//.ovoTraXla, exclusive sale). Though still
used in the sense of the oiuginal Greek, the term is more
accurately applied only to grants from the crown or from
parliament, the private act of an individual whereby he
obtains control over the supply of any particular article
being properly defined as " engrossing." It was from the
practice of the sovereign granting to a favourite, or as a
reward for good service, a monopoly in the sale or manu-
facture of some particular class of goods that the system
of prote(i*ins inventions arose, and this fact lends additional
interest to the history of monopolies (see Patents). When
the practice of making such grants first arose it does not
appear easy to say. Sir Edward Coke laid it down that
by the ancient common law the king could grant to an
inventor, or to the importer of an invention from abroad, a
temporary monopoly in his invention, but that grants in
restraint of trade were illegal. Such, too, was the law laid
down in the first recorded case, Darcy v. Allin (the case of
monopolies, 1602), and this decision was never overruled,
though the law was frequently evaded. The patent rolls
of the Plantagenets show fev.- instances of grants of mono-
polies (the earliest known is temp. Edw. III.), and we
come down to the reign of Henry VIII. before we find
much evidence of this exercise of the prerogative in the
case of either new inventions or known articles of trade.
Elizabeth, as is well known, granted patents of monopoly
so freely that the practice became a grave abuse, and on
several occasions gave rise to serious complaints in the
House of Commons. Lists prepared at the time show that
many of the commonest necessaries of life were the subjects
of monopolies, by which their price was grievously enhanced.
That the queen did not assume the right of making these
grants entirely at her pleasure is shown, not only by her
own statements in answer to addresses from the House, but
by the fact that the preambles to the instruments' convey-
ing the grants always set forth some public benefit to bo
derived from their action. Thus a grant of a monopoly
to sell playing-cards is made, because " divers subjects of
ablo bodies, which might go to plough, did employ them-
selves in the art of making of cards"; and one for ths sale
of starch is justified on the ground that it would prevent
wheat being wasted for the purpose. Accounts of the
angry debates in 1565 and 1601 are given in Hume and
elsewhere. The former debate produced a promise from
the queen that she would be careful in exercising her
privileges ; the latter a proclamation which, received with
great joy by the House, really had but little effect in
stopping the abuses complained of. A few grants were
cancelled, others limited, and others again left to the action
of the ordinary law courts (instead of the privy council).
In speaking of the results of the proclamation, previous
writers seem to have been misled by the promises made in
the queen's speech, promises by no means carried out in
the text of the document itself, a copy of which still exists
in the British Museum.
In the first parliament of James I. a "committee of
grievances " was appointed, of which Sir Edward Coke was
chairman. Numerous monopoly patents were brought up
before them, and were cancelled. Many more, however,
were granted by the king, and there grew up a race of
" pi'.rveyors," who made,use of the privileges granted them
758
I\C O N — M O N
under the great seal for various purposeS'ot extortion. One
oi the most notorious of these was Sir Giles Mompesson,
who fied the r.oimtry to avoid trial in 1621. • After the
intro.U- -ion of several bills, and several attempts by James
to cu'jipromise the matter by orders in council and
promises, the Statute of Monopolies was passed in 1623.
This made all monopolies illegal, except such as might be
granted by parliament, or were in respect of new manu-
factures or inventions. Upon this excepting clause is built
np the entire English system of letters patent for inven-
tions, the statute itself (amended by later Acts) being still
in force. The Act was strictly enforced, and by its aid the
evil system of monopolies was eventually abolished. This
result was not indeed immediately achieved, for (jven during
the Protectorate cases of monopoly patents were brought
!np, and the patents cancelled as grievances. Parliament
has, of course, never exercised its power of granting to any
individual exclusive pi-ivileges of dealing in any articles of
[trade, such as the privileges of the Elizabethan monopolists ;
but the licences required to be taken out by dealers in
wine, spirits, tobacco, itc, are lineal descendants of the old
monopoly grants, while the quasi-monopolies enjoyed by
railways, canals, gas and water companies, &c., under Acts
of Parliament, are also representative of the ancient practice.
MONOTHELITES (iMvoOc\rjrai, monothelitx) was the
name given to those who, in the 7 th century, while other-
wise orthodox, fell into the heresy of maintaining that
Cihrist had only one will The monothelite controversy'
had its origin in the efforts of the emperor Heraclius to
,win back for the church and the empire the excommuni-
cated and persecuted Monophysites or Eutychians of Egypt
and Syria, It seems to have been while in Armenia in
622 .that, in an interview with Paul, the head of the
Severians (Monophysites) there, he first broached the doc-
trine of the /ii'a (vkpyna, of Christ, i.e., the doctrine that
the divine and human natiu-es, while quite distinct in His
one person, had but one activity and operation.! ^t a
somewhat later date he wrote to Arcadius of Cyprus, com-
manding that " two energies " should not be spoken of ;
and in 626, while in Lazistan (Colchis), he had a meeting
with the metropolitan, Cyrus of Phasis, during which this
command was discussed, and Cjtus was at last bidden seek
further instniclion ca the subject from Sergius, patriarch
of Constantinople, a strong upholder of the /ii'a Ivkpyua,
and the emperor's counsellor with regard to it. So well
did he profit by the teaching he received in this quajter
that, in 630 or 631, Cyrus was appointed to the vacant
patriarchate of Aloxandria, and in 633 succeeded in recon-
ciling the Siverians of his province on the basis of /ii'a
diavSpiKT) ivipycia. (one divine-humau energy). He was,
however, opposed by Sophronius, a monk from Palestine,
who, after vainly appealing to Cyrus, actually went to Con-
Btantinoplo to remonstrate with Sergius himself. Shortly
afterwards Sergius -wTote to Pope Honorius, and received
a friendly reply. Sophronius, however, who meanwhile
had been made patriarch of Jerusalem (034), refused to be
silenced, and in his Eputola St/nodi.ca strongly insisted on
the " two energies." So intense did the controversy now
ibecome that at last, towards the end of 638, Heraclius
'published his Edhcsis, or Exposition of the Faith, which
prohibited the use of the phrase " one energy," because of
its disquieting effects on some minds, as seeming to militate
against tlio doctrine of the two natures ; while, on the other
hand, the expression " two energies" was interdicted becau-so
' • Accoiding to some church historians, it was Paul who iutroduced
Iho doctrino ; but this statement seems to rest on a misinterpretation
otthe authoiitica. Sec Hefele, Concilicngeseh. , iii. p. 124 sq. (1877),
who also traces the' previous history of tho CTprcssions ixia. ii'ipytia,
erarSfiicfi (pcfr/fia, especially as fossd Inthe .writings of the Pseudo-
J>in;iy-:ns Arcopa^ta.
it seemed to imply that Christ had two wills. That Christ
had but one will was declared to be the only orthodox
doctrine, and all the faithful were enjoined to hold and
teach it without addition or deduction. The document
was not acceptable, however, to Popes Severinus and John
IV., the immediate successors of Honorius ; and Maximus,
the comcssor, succeeded in stirring up such violent opposi-
tion in North Africa and Italy that, in 648, Constans EL
judged it expedient to withdraw his grandfather's offen.«iv9
edict, and to siibstitute for it his own Typus (rvn-cy; Ttpt
TTtoTtw;), forbidding all discussion of the questions of the
duality or singleness of either the energy or the will of
Christ. Tlie scheme of doctrine of the first four general
councils, in all its vagueness as to these points, was to be
maintained ; so far as the controversy had gone, the dis-
putants on either side were to be held free from censure,
but to resume it would involve penal consequences. The
reply of the Western Church was promptly given in the
unambiguously dyothelite decrees of the Lateran synod
held by Martin I. in 649 ; but the cruel persecutions to
which both Martin and Maximus were exposed, and finally
succumbed, secured for the imperial Typvs the assent at
least of silence. With the accession of Constantine Pogo-
natus in 668 the controversy once more revived, and the
new emperor resolved to summon a genei-al counciL It
met at Constantinople in 680, having been preceded in 679
by a brilliant synod under Pope Agatho at Rome, where it
had been agreed to depart in nothing from the decrees of
the Lateran sjmod. At Constantinople the condemnation
of the monothelite heresy was explicit and complete. Pope
Honorius being anathematized by name along with the
others who had supported it. Beyond the limits of the
empire, monothelism survived for some centuries iu Lebanon
among the Maeonites (?.«'.), w-ho did not abjure their
heresies until 1182.
See the church historians, and especially Hefele {op. cit.\ wUo9»
ounous partisanship can only slightly affect the reader's apprecia-
tion of his full and accurate leaining.
MONEEALE, a contraction of " monte-reale," vas so
called from a jmlace built there by the Norman Roger L,
king of Sicily. It is now a town of about 16,300 inhabit-
ants, situated 5 miles inland from Palermo, on the slope
of Mount Caputo overlooking the beautiful and very fer-
tile valley called " La Concha d'Oro " (the Golden Shell),
famed for its orange, ohve, and almond trees, the produce
of which is exported in large quantities. The town, which
for long was a mere village, owed its origin to the found-
ing of a large Benedictine monastery, ivith its church, the
seat of the metropolitan archbishop of Sicily." This, the
greatest of all the monuments of the wealth and artistic
taste of the Norman kings in northern Sicily, who in 1072
expelled the Mohammedans and established themselves
there wth Palermo as their capital, was begun about 1170
by William II., and in 1182 the chui'ch, dedicated to tho
Assumption of the Virgin Mary, was, by a buU of Pope
Lucius III., elevated to the rank of a metropolitan cathe-
dral. It was, and is even now, one of the most magni-
ficent buildings in the world, and Pope Lucius in no way
exaggerated its splendour when he said in his bull, "ut
simde opus per aliqucm regem factum non fuerit a diebua
antiquis."
The archiepiscopal palace and monastic buildings on the
south side were of gi-eat size and magnificence, and were
surrounded by a massive precinct w all, crowned at intervals
by twelve towera. This has been mostly rebuilt, and but
little now remains except ruins of some of the towers, a
great part of the monlu' dormitory and frater, and the very
splendid cloister, completed about 1 200. This latter is well
- An' earlier cTiurch "appears to have existed at Monreale since tie
6th centurv; but no traces of it now remain.
M 0 N R ,E A L ill
759
preserved, and is one of the finest cloisters both for size
and beauty of detail that now exists anjmhere. It is about
170 feet square, with pointed arches covered mth marble
inlay, supported on pairs of columns ir white marble^ 2X6
^HBiHHH^' ' <BfBBHHIIH
■
Z^Mi N A R T H E X . K|„wipH
A T R 1 U M.
i
■Plan of the cathedral of Monreale, as built in the 12th century,
omitting later additions.
^, 1. Stairs to towers, now altered.
2. Cliapel under the south amho.
S. Staii-s to ambo.
4. Holy-w.ileT stoup.
6, 6. '* Pulpitura " or choir-screen,
! . now destroyed.
.0, fl. Screens behind stalls, now
, destroyed.
,7, 7. Stalls, now destroyed-
8. King's throne.
9. Archbishop's throne.
10, 10. Sanctuary screen.
11. High altar and baldacchino.
12. Altar in northern apse.
13. Altar in southern apse.
14. Altar at tomb of William I.
15. Archbishop's throne.
16, 16. Seats for clergy.
17. Door to great cloister.
18. Door to chapter house.
19. Door to sacristy.
20, 20. Doors to royal palace.
21. Bronze door by'Barisanos.
22. Bronze door by llouauuua.
in all, which are sumptuously decorated either by rich sur-
face carving or by bands of patterns in gold, silver, and
colours, made of glass tesserae, arranged either spirally or
■vertically from end to end of each shaft. The marble caps
are each richly carved with figures and foliage executed
with great skill and wonderful, fertility of invention — no
two being alike. At one angle, a square pillared projection
contains the marble fountain oi monks' laratory, evidently
the work of Moslem sculptors.
The chief feature of the place — the cliurcli — like the main
cloister, ■is fortunately well preserved. .^Jn plan it is 'a'
curious niLxtme of Eastern and Western arraiiijenicnt (."c?
fig.). The nave is like an Italian basilica, while the larj.t
triple-apsed choir is hke one of the early tlu'ec-aiwciV
churches, of which so many examples still exist in S'^yvia
and other Eastern comitries (see D'e Vogue, Si/n'e Cm-
irale). It is, in fact, like two quite different churches put
together end'wise. The basilican nave is wide, with narrow
aisles. Monolithic columns of Oriental granite (excepi
one, which is of cipoUino), evidently the spoils of oldci
buildings, on each side support eight pointed arches uiuch
stilted. There is no t-iforium, but a high clerestory with
wide two-light -windows, ,vith simple tracery like those in
the aave- aisles and throughout the church. . The othci
half, Eastern in two senses, is both wider and higher than
the nave., Tt also is divided into a central space with two
aisles, each of the divisions ending at the east with an
apse. The roofs throughout are of open woodwork verj
low in pitch, -constructionally plain, but richly decorated
with colour, now mostly restored. At the west end o)
the nave are two projecting towers, with narthex-entrance
between them. A large open atrium, which once existec
at the west, is now completely destroyed. The outside ot
the church is plain, except the aisle walls and three eastern
apses, which are decorated with intersecting pointed arches
and other ornaments inlaid in marble. The outsides ol
the principal doorways and their pointed arches are magni-
ficently enriched ■with carving and inlay, a curious com-
bination of three styles — Norman-Freuch, Byzantine, and
Arab.
It is, however, the enormous extent (80,630 square feet)
and glittering splendour of the glass rhosaics covering the
interior, which make this church so marvellously splendid
(see Mosaic). With the exception of a high dado, itself
very beautiful, made of marble slabs enriched with bands of
mosaic, the whole interior surface' of the walls, including
soffits and jambs of all the arches, is covered -with minute
mosaic-pictures in brilliant colours on a gold ground. This
gorgeous method of decoration takes the place of all purely
architectural detail, such as mouldings and panelling.
The mosaic covers even the edges of the arches and jambs,
which are slightly rounded off, so as to allow them to bo
covered by the glass tesserae. This device gives apj>arent
softness to all the edges, and greatly enhances the richness
of effect produced- by the gleaming gold grounds. Th^
only carving inside is on the sculptured caps of the nave
arcade, mostly Corinthian in style. The mosaic pictures
are arranged in tiers, divided by horizontal and vertical
bands of elaborate flowing mosaic ornament. In i^arts ol
the choir there are five of these tiers of subjects or single
figures one above another. The half dome of the central
apse has a colossal half-length figure of Christ, with a
seated Virgin and Child below ; the other apses have full-
length colossal figures of St Peter and St Paul. Inscrip--
tions on each picture explain the subject or saint repre-
sented ; thes;2 are in Latin, except some few which are
in Greek. The subjects are partly from the .Old Testa-
ment tyjies of Christ and His scheme of redemption, with
figures of those who prophesied and prepared for^-His
coming. Towards the east are subjects from the New
Testament, chiefly representing Christ's miracles and suffer-
ing, -with apostles, evangelists, and other saints. . Tha
design, execution, and choice of subjects all appear to be'
of Byzantine origin, the subjects being selected from the
Menologium drawn up by the emperor Basilius Porphyro-.
genitus in the 10th century.
No other mosaics perhaps' so closely resemble the Mon-
ceo
M 0 N — M O M
reale ones us thoas over the nave columns in the Church
of the Kativity at Bethlehem. They are alike, not only
in design and treatment, but also in the curious mixture
of Latin and Greek in the inscriptions (see De Vogue,
£ijlises de la Ter,e Sainte, 1860). This similarity is easily
accounted for by the fact that these two sets of mosaics,
though 60 far apart, were executed about the same date
and under the same conditions, viz., by the hands of
Byzantine artists, working for Norman-French kings.
Ij the central apse at Mbnreale, behind the high altar,
kj a fine maible throne for the archbishop. This position
of the tiirone is. a survival of the early basilican arrange-
ment, when the apse and altar were at the west end. In
that case the celebrant stood behind the altar at mass, and
looked over it eastwards towards the people. This posi-
tion of the throne was frequently reproduced in churches
which, like this, have the apse at the east. On the north
side, in front of the high altar, is another somewhat
similar throne for the use of the king. The tomb of
William L, the founder's father — a magnificent porphyry
sarcophagus contemporary with the church, under a marble
pillared canopy — and the founder William 11. 's tomb,
erected in 1575, were both shattered by a fire, which in
1811 broke out in the choir, injuring some of the mosaics,
and destroying all the fine walnut choir-fittings, the organs,
and most of the choir roof. The tombs were rebuilt, and
the whole of the injm-ed part of the church restored,
mostly very clumsily, a few years after the fire. On the
north of the choir are the tombs of Margaret, wife of
William I., and her two sons Eoger and Henry, together
with an urn containing the viscera of St Louis of France,
who died in 1270. The pavement of the triple choir,
though much restored, is a very magnificent specimen of
marble and porphjrry mosaic in "opus Alexandrinum," with
signs of Arab influence in its main lines.
Two bronze doors, those on the north and west of the
church, are of great interest in the history of art. They
are both divided into a niunber of square panels with sub-
jects and single figures, chiefly from Bible history, cast in
relief. That on the north is by Barisanos of Trani in
southern Italy, an artist probably of Greek origin. It is
inscribed baeisanus than, me fecit. The cathedrals at
Trani and Ravello also have bronze doors by the same
sculptor. The western door at Monreale, inferior to the
northern one both in richness of design and in workmanship,
is by Bonanuus of Pisa, for the cathedral of which place
he cast the still existing bronze door on the south, opposite
the leaning tower. The one at Monreale is inscribed a.d.
MCIXXXVI IND. m. BONANNUS CIVIS PISANVS ME FECIT.
It is superior in execution to the Pisan one. The door by
Barisanos is probably of about the same time, as other
examples of his work with inscribed dates show that he
was a contemporary of Bonannus. (See Metal-wokk.)
The monastic Hbrary contains some valuable MSS., especi-
ally a number of bilingual documents in Greek and Arabic,
the earliest being dated 1144. The archbishop now occu-
pies the eastern part of the monastic buildings, the original
palace being destroyed.
See Serradifako, Vitamo di llormah, lie, 1338 ; Gravina,2)«omo
(/> Monreale, the best work on tho subject, 1859 *7. ; Testa f^ila
del He Quglielmo 11., 1765 ; Tarailo, / Rcali Scpolcri di Mon-
reale, 1826 ; Hittorf ot Zaiith, Architecture de la Sicile, 1835 ■
Gaily Knipht, Saraeenie and Norman Hcmnins in Sicihj, London'
18-10 ; W. Burges, Notes oh llcdiseml Jfosaic, 1863 ; M. D. Wyatt'
Mosaics of Middle Ages, London, 1849 ; Hcssemcr, Arahisdie und
Alt-ltalienische Bau-Ver:nerungen, 1853 ; Garrucci, Arte Cristiana
^882. (J. H. M.) '
MOITEOE, James (17D8-1831), fifth president of tho
United States, was born 28th April 1758, in the county
of Westmoreland, Virginia. According to the family
tradition, their ancestors are traced back to a family of
Scottish cavaliers descended from Hector Monroe, an officer
of Charles L At the outbreak of the Revolut-onary war,
James Monroe was a student at the College of William and
Mary, but left his studies in 1776 to join the continental
army. He took part as lieutenant in the New Jersey
campaign of that year, and was wounded at the battle of
Trenton. The next year he served with the rank of captain
on tho staff of General William Alexander ("Lord Stirling"),
but, thus being out of the line of promotion, he soon found
himself without military employment. In 1780 he began
the study of the law under the direction of Jefferson, then
governor of Virginia. His intimacy with Jefferson at this
time had probably a controlling influence upon his subse-
quexit political career. He continued through all vicissitudes
to possess the friendship and support of both Jefferson and
Madison.
In 1782 Monroe was in the State legislature, and from
1783 to 1786 was a member of Congress. On retiring
from Congress he entered upon the practice of the law at
Fredericksburg, and was again elected to the legislature.
In the Virginia convention of 1788 for the ratification of
the constitution, he was among the opponents of that
instrument ; but his course was approved by the legisla-
ture of his State, who elected him United States senator
in 1790 to fill the vacancy caused by the death of William
Grayson. As senator he was a decided opponent of the
Federalist administration. Nevertheless he was selected
by Washington in 1794 as minister to France in place of
Gouverneur Morris, a Federalist, recalled upon the request
of the French Government. Being of the party who sym-
pathized with the revolutionary struggle in France, it was
expected that his appointment would be flattering to the
Government of that country, and would also conciliate the
French party at home. The Government of the National Con-
vention received Monroe with open signs of favour, and on
his part he expressed his own and his country's sympathy
with the French Republic with so much enthusiasm that
Washington deemed his language not in keeping with the
neutral policy which the administration had recently pro-
claimed. At about the same time John Jay had negotiated
a treaty of amity and commerce with England which gave
great umbrage to France. It was alleged that the earlier
treaty of 1778 with France was violated by the stipulations
of the Jay treaty ; and the Directory seemed disposed to
make of this a casus belli. In this emergency it was
believed by Washington and his advisers that Jlonroe
failed to represent properly the policy of the Government,
and he was therefore recalled in 1796. In justification of
his diplomatic conduct, he published the next year his
View, a pamphlet of 600 pages. In 1799 he became
governor of Virginia, and was tvdce re-elected. In the
meantime the Keimblican party had come into power, with
Jefferson as president, and Monroe was again called upon
to fill an important diplomatic station. He was com-
missioned on 10th January 1803 to act with Livingston,
resident minister at Paris, in negotiating the purchase of
New Orleans and the territory embracing the mouth of
the Mississippi, wliich formed a part of the province of
Louisiana, recently ceded by Spain to France. In view of
the anticipated renewal of hostilities between England and
France in 1 803, Napoleon was anxious, for a consideration,
to part with his new acquisition, which in the event of a
war with England he would probably lose by conquest.
The American commissioners met therefore with little
difliculty in the accomplishment of their object. But, in
the absence of instructions, they assumed -the responsibility
of negotiating the purchase not only of New Orleans but
of tho entire territory of Louisiana — an event that is hardly
second in importance to any in the history of the countrr
Monroe was next commisiioaed as minister to Englw'il,
M O N — M 0 N
761
to gncceed Unfns King, who had resigned. In 1801 he
undertook a mission to Madrid, with the object of
negotiating the purchase of the Floridas ; but in this he
was unsuccessful, and returned to London in 1S05. The
next year he was joined in a commission with William
Pinkney to negotiate a treaty with England to take the
place of the Jay treaty, which expired in that year.
Lords Auckland and Howick having been appointed on the
part of England, a treaty was concluded on the last day
of the year, which was perhaps more favourable to the
United States than the Jay treaty ; but, like the latter, it
contained no provision against the impressment of Ameri-
can seamen. For this reason President Jefferson refused
to submit it to the Senate for ratification, but sent it back
for revision. In the meantime Canning had become
foreign secretary in place of Fox, and refused to re-
open the negotiation. Monroe returned to the United
States in 1807, and, as in the case of his first French
mission, he drew up a defence of his diplomatic conduct
in England. In 1808 certain disaffected Republicans
attempted to put Monroe forward as the candidate for the
Presidency, but as Virginia declared in favour of Madison
Monroe withdrew his name. In 1810 he was again in
the legislature of his native State, and the next year its
governor. But in this year he was called from the state
to the national councils, superseding Robert Smith as
secretary of state in Madison's cabinet, and took an
active part in precipitating the war against England in
1812. On the retirement of Armstrong, after the capture
of Washington in 1814, Monroe assumed the duties of the
war department in addition to those of the state depart-
ment, and by his energy and decision infused something
of vigour into the conduct of the war. He was elected
president in 1816, and was re-elected in 1820 without
opposition. The period of his administration (1817-25)
has been called " the era of good feeling," for the reason
that the party issues of the past were mostly dead, and
new issues had not yet arisen. In the formation of
his cabinet Monroe showed the soundness of his judg-
ment, selecting for the leading positions J. Q. Adams,
J. C. Calhoun, W. H. Crawford, and William Wirt. With
these able advisers he devoted himself to the economic
development of the country, which had been so long
retarded by foreign complications. As president, more-
over, he was able to accomplish in 1819 the acquisi-
tion of the Floridas, which as minister to Spain he had
failed to do in 1804, and to define the bovmdary of Louis-
iana, which he had been the agent in purchasing in 1803.
But Monroe is best known to later generations as the
author of the so-called " Monroe doctrine," a declaration
inserted in his seventh annual message, 2d December 1823.
It was the formulation of the sentiment, then beginning
to prevail, that America was for Americans. One of the
principles of the neutral policy of the country, which had
been established with much difficulty, had been that the
United States would not interfere in European politics ;
and now this policy was held to include the converse as a
necessary corollary — that is, that Europe should not inter-
fere in Ajjierican politics, whether in North America or South
America-iJ^The occasion of proclaiming this doctrine was
the rumoured intervention of the Holy Alliance to aid Spain
in the reconquest ' of her American colonies. President
Monroe believed that such a policy entered upon by the
allied continental powers of Europe would be dangerous
to the peace and seufety of the United States ; he therefore
declared that "we would not view any intervention for
the purpose of oppressing them (the Spanish American
states) oi'cont'roUiiig in any manner their destiny, by any
European power, in any other light than as the manifesta-
tion of an unfriendly disposition towards the United
States." This declaration, together with the known hos.
tility of England to such a project, was sufficient to prevent
further action on the part of the Alliance.
On the expiration of his presidential term Monroe re-
tired to Oak Hill, his residence in London county, Vir-
ginia ; but at the time of his deatji, 4th July 1831, he was
residing in New York. He was married about 17SC, and
left two daughters. He was a man of spotless character ;
and, though not possessing ability of the first order, he
ranks high as a wise and prudent statesman. His Life
has been written by D. C. Gibnan. (f. sn.)
MONROE, a city of the United States, cormty seat of
Monroe county, Michigan, lies 32 miles south-south-west
of Detroit, on both banks of the Raisin river, 3 miles
inland from Lake Erie, with which it has been connected
by a ship-canal since 1843. It is a station on the Canada
Southern, the Flint and Pere Marquette, and the Detroit
division of the Lake Shore and Michigan Southern Rail
ways. Agricultural implement factories, a spoke and hull
factory, f — -.dries and engineering-works, carriage-wcrks,
grist-miUs, paper-mills, and fniit-drying establishments ore
in operation. From 400 to 500 tons of grapes are shipped
yearly from the neighbouring vineyards, and over 100,000
gallons of wine are made here. The population in ISSO
was 4928. Settled as Frenchtown by a body of Canadians
in 1784, Monroe received its present name, in honour of
President Monroe, in 1817. Its city charter dates from
1837. It was the scene of the battle of the river Raisin,.
22d January 1813.
MONROVIA. See Liberia, voL xiv. p. 608.
MONS, a town of Belgium, the capital of the proTince
of Hainault, on the rivers Haine and Trouille, and 31
miles south-west of Brussels. The population in 1880 was
25,600. Mons is divided by the river Trouille into an
upper and lower town, the first built on rising ground in
the shape of an amphitheatre, the second extending into the
plain ; four bridges connect the two. The place is pleasing
and cheerful of aspect, having broad weU-paved streets
and handsome squares. The fortifications, once among the
strongest of the Continent, have quite recently been razed,
their site being now occupied by an extensive avenue or
boiilevard. Among the monuments worthy of mention
are — the church of St Waudru, one of the best types of
original architecture to be found in Belgium ; the church
of St Elizabeth, a combination of the Gothic style and
the Corinthian; the town-hall, erected in 1458; and the
belfry tower, next to which formerly rose the old castle
of the counts of Hainault, the demolition of which led,'
a few years ago, to the discovery of some curious mural
paintings belonging to the 12th century. Mons possesses
a military arsenal, a school of engineering, and a public
library of importance; the administration of law and
government for the province is concentrated there. It
contains manufactures of cotton, velvet, cloth, muslin,
soap, and clay pipes ; also brass-foundries, tan-yards, and
breweries, and a market of some note for agricultural
produce, cattle, horses, and tobacco. The main source of
the wealth and prosperity of Mons is derived from the
collieries which exist in its vicinity, and yield annually
between two and three million tons of first-class coal, the
greater part of which is carried into France ; in the imme-
diate neighbom-hood of the town are the large and important
villages of Jemmapes, Quaregnon, Frameries, Paturages,
Wasmes, and Dour, each with a population of from ten to
twelve thousand inhabitants; these locaU ties, together with
many others somewhat less peopled, form an agglomeration
called the Borinage, rich in coal-mines, in iron-foundries, in
stone and marble quarries, and may be considered as one
of the busiest centres in the world.
Mons is built on the site of a Koman camp erected by JvJiua
762
M 0 N — M O N
C^.-mr, and aftcrwar(Js occiipiDd by a brotlicT of Cicero, who was
besiegwl there by Ambiorix ^hief of the Eburoues. In the 8th cen-
tury a lady of the name of Waudru or Waltrud, countess of Hain-
»olt, founded a convent, which became the centre of the town. In
804 Charlemagne made it the capital of the county of Hainault ; it
was fortified in 1H8. Baldmn VI., afterwards Latin emperor of
Constantinople, was very active in promoting the interests of Mous,
and endowed it with a celebrated charter in the year 1200. After
teing reduced by nearly one half by the plague, Mons received
within its walls the Jews whom Philip the Long had expelled from
France. The city attained its highest degree of prosperity under
pharles V., but its greatness w.-is arrested during the goverriment
jf the duke of Alva by civic disturbances, which lasted until the
reign of Albert and Isabella. In more recent times Mons has had
to pay tribute to the warlike spirit of its neighboui's ; it was taken
ijy Louis XIV. in 1691, given back in 1697, and retaken in 1701 and
»gain in 1709. In 1748 it fell into the hands of Austiia ; the Belgian
insurgents stormed it in 1789 ; the French iu 1792, when Dumouriea
won the battle of Jemmapes under its walls ; ia 1814 it belonged
to the Netherlands, and has formed part of the Belgian kingdom
3mce 1830.
MONSOON. See Meteoeology, supra, p. 148 sj., and
Inbi.uj Ocean.
MONSTER. Monsters or naonstrous births are tlie snb-
ject of Animal Teratology, a department of morphological
science treating of deviations from the normal development
of the embryo. The term "embryo" is conventionally
limited, in human anatomy, to the ovum in the first three
months of its intra-uterine existence, v,-hile it is still develop-
ing or acquiring the rudiments of its form, the term
"f cetus" being applied to it in the subsequent months during
which the organism grows on the lines of development
already laid dowsi. It is mostly in the first or embryonic
jperiod that those deviations from the normal occur which
present themselves as monstrosities at the time of birth ;
these early traces of deviation within the embryo may be
slight, but they " grow with its gro^vth and strengthen with
its strength," until they amount to irreparable defects or
secretions, often incompatible with extra-uterine life. The
name of " teratology," introduced by fitienne Geoffroy St-
Hilaire (1822), is derived from ripas, the equivalent of
. monstrum ; teratology is a term new enough to have none
but scientific associations, while the Latin word has a long
record of superstitions identified ■nith it. The myths of
siren, satyr, Janus, cyclops, and the like, with the cor-
responding figures in Northern mythology, find a remote
anatomical basis in monstrosities which have, for the most
part, no life except in the foetal state. The mythology of
giants and dwarfs is, of course, better founded. The term
monster was originally used in the same sense as portent :
Ci<:&m{De Div.,\.)&a.ys.," Moiistra,ostenta,poHenta,prodigia
appellantur, guoniam monslrant, ostendvnt, portendunt, et
pradicunt." Luther ^ speaks of the birth of a monstrous
calf, evidently the subject of contemporary talk, as pointing
to some groat impending change, and he expresses the hope
that the catastrophe might be the Last Day itself. The
rise of more scientific views will be sketched at the close
of the article
Although monstrosities, both in the human species and
in other animals, tend to repeat certain definite types of
erroneous development, they do not fall readily into classes.
It is remarked by Vrolik that a scientific classification is
impracticable from being too cumbrous, and that a con-
venient grouping is all that need be attempted. The
most usual grouping (originally suggested by Bufibn, 1800)
is into monstra per excesmm, monstra per defectum, and
monUra per fabricaTh alienam. It seems iiseful, ho'yever,
to place the more simple cases of excess and of defect side
by side; and it is necessary, above all, to separate the
double monsters from the single, the theory of the former
being a distinct chapter in teratology^
'^ 1 In a passogc quoted by BischoIT from the lOtli volume ot UutUcT'o
Forks, Hallo ed., p. 24!<i.
1. Monstrosities in a Singh Sody. — The abnormality
may extend to the body throughout, a.s in well-proportioned
giants and dwarfs ; or it may affect a certain region or
member, as — to take the simplest case — when there is a
finger or toe too many or too few. It is very common
for one malformation to be correlated with several others,
as in the extreme case of acardiac monsters, in which the
non-development of the heart is associated with the non-
development of the head, and with other radical defects.
Giants are conventionally limited to persons over 7
feet in height. The normal proportions of the frame
are adhered to more or less closely, except in the skidl,
which is relatively small ; but accurate measurements,
even in the best-proportioned cases, prove, when reduced
to a scale, that other parts besides the skull, notably
the thigh-bono and the foot, may be undersized though
overgroivn." In persons who are merely very tall, the great
stature depends often on the inordinate length of the lower
limbs ; but in persons over 7 feet the lower limbs are not
markedly disproportionate. In many cases the muscles
and viscera are not sufficient for the overgrown frame, and
the individuals are usually, but not always, of feeble
intelligence and languid disposition, and short-lived.'
The brain-case especially is undersized — the Irish giant
in the museum of Trinity College, DubUn, is the single
exception to this rule — but the bones of the face, and'
especially the lower jaw, are on a large scale. Giants
are never born of gigantic parents ; in fact, sterility
usually goes with this monstrosity. ' Their size is some-
times excessive at birth, but more often the indications of
great stature do not appear till later, it may be as late as
the ninth year; they attain their full height before the
twenty-first year. They have been more frequently male
than female; the German giantess lately exhibited (1882)
was as tall as any authentic case in the male sex.
Dwarfs are conventionally limited to persons under 4
feet. They are more Ukely than giants to have the modu-
lus of the body perfect. * " In the true dwarf, as far as I
have been able to ascertain, the proportions between the
several parts of the frame are good, corresponding, or
nearly corresponding, with those of the noimal adult ; and
the diminutive stature depends, accordingly, not upon re-
latively imperfect growth of any particidar segments, or
even upon the permanepce of a foetal or childlike con-
dition, but upon the whole frame being tmdersized "
(Humphry). ^Vhere disproportion occurs in the true,
dwarf it takes the form of a large-sized head, broad
shoulders and capacious chest, and undersized lower limbs.
Dwarfs with rickets are perhaps to be distinguished from
true dwarfs ; these are cases in which the spine is curved,
and sometimes the bones of the limbs bent and the
pelvis deformed. As in the case of giants, dwarfs are
seldom the progeny of dwarfs, who are, in fact, usually
sterile ; the unnatural smallness may be obvious at birth,
but is more likely to make itself manifest in the years of
growth. Dwarfs are much more easily brought up than
giants, and are stronger and longer -lived ; they have
usually also strong passions and acute intelligence. The
legends of the dwarfs and giants are on the whole well
based on fact (see Dwaef and Giant).
Redundancy and Defect in Single Parts. — The simplest
case of tliis redundancy is a sixth digit, well formed, and
provided with muscles (of tendons), nerves, and blood-
vessels like the others ; it is usually a repetition of the little
finger or toe, and it may bo present on one or both hands,
or on one or both feet, or in all foiu' extremities, as in the
giant of Gath. The want of one, two, or more digits on
hand or foot, ax- on both, is another fiiniple auoioaly ; and,
' S«c the lajtfs in TlmnpTir^i's flvatire on the .Jtwiaa Skdeton, p. 109. .'
MONSTER
763
like tlio redundancy, it is apt to repeat itself in the
same family. Meckel saw a giil who had an extra digit
on each extremity, while a sister wanted four of the fingers
of one hand. Where the supernumerary digits are more
than one on each extremity, the whole set are apt to be
rudimentary or stunted ; they look as if two or more of tho
embryonic buds had been subject to cleavage down the
middle, and to arrest of longitudinal growth. There are
two or three authentic instances of a whole lower limb ap-
pearing at birth as two withered halves, as if from embry-
onic cleavage.^ Other redundancies of the skeleton are
extra vertebrae (sometimes the coccygeaJ, giving the ap-
pearance of a rudimentary tail), or an extra rib. A
double row of teeth is occasionally met with ; the most
interesting case of this anomaly is .that in which the
rudiments of a double row exist from the first, but the
plienomenon is sometimes produced by the milk teeth
persisting along with the second set. One or more extra
teeth are occasionally met with in iine with the rest.
Among redimdancies of the soft parts, by far the most
frequent is an extra nipple, or pair of nipples. It is only
the nipple, or the most external mechanical adjunct of the
mammary apparatus, that is repeated, and very seldom, if
ever, the breast structure itself. The nipple, althougk it is
the latest addition to the mechanism of lactation, is in the
individual mammal developed on the skin before the gland
is formed underneath ; and that facility, which applies to
the development of external characters generally, appears
to be the reason why there may be one or more extra
nipples but no redundant gland. lu the same connexion,
it is interesting to observe that the supernumerary nipple,
has been shown by statistics on a large scale to be twice as
common in men as in women, although in the male the
mammary function never comes to maturity, and even the
structme retrogrades after puberty. Traces of an additional
nipple, or pair of them, in more or less symmetrical position
below the normal ones, are not very uncommon when care-
fully looked for. Among the sense organs there is a
remarkable instance recorded of doubling of the appendages
of the left eye, but not of the eyeball itself ; the left half
of the frontal bone is double, making two eye-sockets on
that gide, and the extra orbit has an eyebrow and eyelid. ^
The external ear (jjinna) has also been found double on one
side. Doubling of any of the internal organs is extremely
rare, and is probably always traceable to a more or less
complete Assuring or lobation. The ducts or vessels con-
nected with organs, and playing a purely mechanical part,
are not unfrequently doubled ; thus each kidney may have
two ureters, and a similar variation may occur in veins
am! arteries.
Monstrosities from Defective Closure in the Middle Line.
Under this head come some of the commonest congenital
malformations, including slight deficiencies such as luireUp,
and serious defects such as a gap in the crown of the
head with absence of the brain. The embryo is originally
a cLcular flattened disc spread out on one pole of the yolk,
and itisformtdintoacyUndrical body (vrith four appendages)
by the free margins of the disc, or rather its ventral laminse,
folding inwards to meet in the middle line and so close in
the pelvic, abdominal, thoracic, pharyngeal, and oral cavities.
Meanwhile, and indeed rather earlier, two longitudinal
parallel ridges on the top or along the back of the disc
have grown up and united in the middle line to form the
second barrel of the body— the neural canal— of smaU and
uniform width in the lower three-fourths or spinal region,
but expanding into a wide chamber for the brain. This
division into neural (dorsal) and hsemal (ventral) canals
' See Foretet's AUiu, Taf. vui., figs. 13 and li
' See preparatioD in the Wuisbuig ilUMum, Sgiircd by Fo.-aler, Tat
TUL, DgS. 9-12.
underlies all vertebrate development. Impenect closure
along either of those embryonic lines of junction may prtv
duce various degrees of monstrosity. The simplest and
commonest form, hardly to be reckoned in the present cate-
gory, is harelip with or without cleft palate, which results
from defective closure of tho ventral laminoe at their extreme
upper end. Another simple form, but of much more serious
import, is a gap left in the neural canal at its lower end j
usually the arches of the lumbar vertebrae are deficient,
and the fluid that surrounds the spinal cord bulges out ii^
its membranes, producing a soft tumour under the skin at
the lower part of the back. This is the condition known
as hydrorhachis, depending on the osseous defect knovra as
spina bifida. Children bom with this defect are difficult
to rear, and are very likely to die in a few days or weeks.
More rarely the gap in the arches of the vertebrae is in the
region of the neck. If it extend all along the back, it will
probably involve the skuU also. Deficiency of the crown
of the head, and in the spine as well, may be not always
traceable to want of formative power to close the canal in
the middle line ; an over-distended condition of the central
water-canal and water-spaces of the cord and brain may
prevent the. closure of the bones, and ultimately lead to
the disruption of the nervous organs themselves ; and
injuries to the mother, with inflammation set up in the
foetus and its appendages, may be the more remote cause.
But it is by defect in the middle line that the mischief
manifests itself, and it is in that anatomical category that
tho malformations are included. The osseous deficiency
at the crown of the head is usually accompanied by want
of the scalp, as well as of the brain and membranes. Tlie
bones of the face may be well developed and the features
regular, except that the eyeballs bulge forward under, the
closed lids ; but there is an abrupt horizontal line above
the orbits where the bones cease, the skin of the brow
joining on to a spongy kind of tissue that occupies the
sides and floor of the cranium. This is the commonest
foi-m of an aneneephaloxts or brainless monster. There are
generally mere traces of the brain, although, in some rare
and curious instances, the hemispheres are developed in
an exposed position on the back of the neck. The cranial
nerves are usually perfect, with the exception sometimes
of the optic (and retina). Vegetative existence is not im-
possible, and a brainless monster has been kno.vn to
survive sixty-five days. The child is usually a very large
one.
Closely allied, as we have seen, to the anencephalous
condition is the condition of congenital hydrocephalus.
The nervous system at its beginning is a neural canal, not
only as regards its bony covering, but in its interior ; a
wide space lined by ciliated epithelium and filled with
water extends along the axis of the spinal cord, and
expands into a series of water-chambers in the brain. As
development proceeds, the walls thicken at the expease of
the internal water-spaces, the original tubular or chambered
plan of the central nervous system is departed from, and
those organs assume the practically solid form in wnich
we familiarly know them. If, however, the water-spaces
persist in their embryonic proportions notwithstanding
the thickening of the nervous substance forming their
walls, there results an enormous brain which is more than
half occupied inside with water, contained in spaces that
correspond on the whole to the ventricles of the brain
as normally bounded. A hydrocephalic foetus may sur-
vive its birth, and will be more apt to be affected in its
nutrition than in its intelligence. In many cases the
hydrocephalic condition does not come on till after the\
child is bom. The microceplicUous condition, where it is
not a part of cretinism, is not usually a congenital defect
in the strict Bensii. but more often a conseauence of tho
764
M O- N S T K R
premature union of tlie bones of the skull along their sutures
or lines of growth.
Eeturning to the ventral middlef line, there may be
defects of closure below the lips and palate, as in the
breast-bone (fissure of the sternum), at the navel (the last
point to close in any case), and along the middle line of
the abdomen generally. The commonest point for a gap
in the nuddle line of the belly is at its lower jiart, an iuch
'or two above the pubes. At that point in the embiyo
there issues the allantois, a baUocn-Iibe expansion from
the ventral cavity, which carries on its outer surface
blood-vessels from the embryo to interdigitato with those
,of the mother on the uterine surface. Having served its
temporaiy purpose of carrying the blood-vessels across a
space, the balloon-like allantois collapses, and rolls up into
the rounded stem-like umbilical cord through most of its
extent ; but a portion of the sac within the body of the
fcetus is retained as the permanent' urinaty bladder: That
economical adaptation of a portiot; of a vesicular organ,
origiiially formed for purposes of communication between
the embryo and the mother, appears to entail sometimes
a defect in the wall of the abdomen jvist above the pubes,
and a defect in the anterior wall of the bladder itself.
This w the distressing congenital condition of fissure of
the urinary bladder, in which its interior is exposed
through an opening in the skin; the pubic bones are
separated by an interval, and the reproductive organs are
ill formed ; the urachus is wanting, and the imibUicus is
always placed exactly at the upper end of the gap in the
skin. A monstrosity recalling the cloacal arrangement
cf the bird is met with as a more extreme defect in the
same parts.
Hermaphroditism. — Although this anomalous condition
does not fall imder defective closure in the middle line, it
may ba said to be due to a similar failiu-e of purpose, or to
an uncertainty in the nisus formativus at a corresponding
stage of development. There is a point of time, falling
about the eighth week, up to which the embryo may de-
velop either the reproductive organs of the male or the
reproductive organs of the female ; in the vast majority of
cases' the future development and growth are carried out on
one line or the other, but in a small number there is an
ambiguous development leading to various degrees of
hermaphroditism or doubtful sex. The primary indecision,
so to speak, affects only the ovary or testis respectively,
cr rather the common germinal ridge out of which either
may develop ; the uncertainty in this embryonic sexual
ridge sometimes leads actually to the formation of a pair
of ovaries and a pair of small testes, or to an ovary on one
side and a testis on the other ; but even when there is no
such double sex in the essential organs (as in the majority
of hermaphrodites) there is a great deal of doubling and
ambiguity entailed in the secondary or external organs and
parts of generation. ThosQ parts which are rudimentary or
obsolete in the male but highly developed in the female,
and those parts which are rudimentary in the female but
highly developed in the male tend in the hermaphrodite
to bo developed equally, and all of them badly. In
some cases the external organs of one sex go with the
intemai organs of the opposite sex. It has been observed
thatwhen middle life is reached or passed the predominance
in features, voice, and disposition leans distinctly towards
the masculine side. The mythological or clae^ical notions
of hermaphroditism, like so much else in the traditions of
teratology, are exaggerated.
Cyclops, Siren, itc. — The same feebleness of the forma-
tive energy (the Bildungstrieb of Blumenbach) which gives
rise to some at least of the coses of defective closur* ia
the middle line, and to the cases of undecided sc.x, leads also
to imperfect separation of syuimetricai earts. The most
remarkable case of the kind is the cyclops monster. At
a point corresponding to the root of the nose there is
found a single orbital cavity, sometimes of small size and
with no eyebaU in it, at other times of the usual size of
the orbit and containing an eyeball more or less complete.
In still other cases, which indicate the nature of the
anomaly, the orbital cavity extends for some distance on
each side of the middle line, and contains two eyeballs lying
close together. * The usual nose is wanting, but above the
single orbital cavity there is often a nasal process on the
forehead, with which nasal bones may be articulated, and
cartilages joined to the latter ; these form the framework
of a short fleshy protuberance- hie a small proboscis.
The lower jaw is sometimes wanting in cyclopeans ; the-
cheek-bones are apt to be small, and the mouth a small
round hole, or altogether absent ; the rest of the body may
be well developed. The key to the cyclopean condition
is found in the state of the brain. The olfactory nerves
or lobes are usually described as absent, although Vrolik
has found them in some instances ; the brain is very imper-
fectly divided into hemispheres, and appears as a somewhat
pear-shaped sac with thick walls, the longitudinal partition
of dura mater (falx cerebri) being wanting, the surface
almost unconvoluted, the corpus callosum deficient, the
basal ganglia rudimentary or fused. The optic chia^ma
and nerves are usually replaced by a single mesial nerve,
but sometimes the chiasma and pair of nerves are present.
The origin of this monstrosity dates back to an early
period of development, to the time when the future
hemispheres were being formed as protrusions from the
anterior cerebral vesicle or fore-brain ; it may be conceived
that, instead of two distinct buds from that vesicle, there
was only a single outgrowth with imperfect traces of cleav-
age. That initial defect would carry -with it naturally the
undivided state of the cerebrum, and with the latter there
would be the absence of '"ilfactory lobes and of a nose, and
a single eyeball placed where the nose should have been.
A Cyclops has been known to live for several days. The
monstrosity is not uncommon among the domestic animals,
and is especially frequent ia the pig. There is another
congenital malformation, in which an eyeball is wanting
from one of the sockets ; but in that case there is no defect
of development in the bones, and the brain ttnd nose are
normal.
Another ciurfous result of defective separation of sym-
metrical parts is the siren form of foetus, in which the
lower limbs occur as a single tapering prolongation of the
trunk like the hinder part of a dolphin, at the end of
which a foot (or both feet) may or may not be visible.
The defects in the bones underlying thi.^ siren form are
very various : in some cases there is only one limb (Ihigh'
and leg-bones) in the middle line ; in others all the bones
of each limb are present in more or less rudimentary
condition, but adhering at prominent points of the ad-
jacent surfaces. The pelvis and pelvic viscera share in the
abnormality. A much more common and harmless case of
unseparated symmetrical parts is v>here the hand or foot
has two, three, or mora digits fused together. This syn-
dactylous anomaly runs in families,
lAmhs Absent or Stunted. — -Allied to these fused or un-
separated states of the extremities, or of parts of them,
are the class of deformities in which whole linbs are
absent, or represented only by stumps. The trunk (and
head) may be well formed, and the individual healthy ;
all four extremities may be reduced to short stumps eitEer|
wanting hands and feet entirely, or with the latter fairly
well developed; or the legs only may be rudimentary or
wanting, or' the arms only, or one extremity only. Al-
though some of these cases doubtless depend upon aber-l
rant or deficient formative power in the particular direo*
M G N S T E B
765
tions, there wo others of them referable to the effects of
mechanical pressure, and even to direct . amputation of
parts within the uterus.
Aeardiac and Acranial Moiuten. — It sometimes uappens
in a twin pregnancy that one of the embryos fails to
develop a ' heart and a complete vascular system of its
own, depending for its nourishment upon blood derived
from the placenta of its well-formed twin by means of its
umbilical vessels. It grows into a more or less shapeless
mass, in which all traces of the human form may be lost.
Other viscera besides the heart will be wanting, and
no head distinguishable j the most likely parts to keep
the line of devSopment are the lumbar region (with the
kidneys), the pelvis, and the lower limbs. The twin of
this monster may be a healthy infant.
Reversed Position of the Viicera. — ^This is a develop-
mental error depending on the retention of the right aortic
arch as in birds, ini>tead of the left as is usual in mammals.
The position of all the unsymmetrical viscera is transposed,
the spleen and cardiac end of the stomach going to the
right side, the liver to the left, the cecum resting on the
left iliac fossa, and the sigmoid flexure of the colon being
attached to the right. This condition of tiltie. inversus
viscemm need cause no inconvenience ; and it will probably
remain undetected until the occasion should arise for a
physical diagnosis or post-mortem inspection. There are
numerous other anomalies in the development of the great
vessels. In the heart itself there may be an imperfect
septum ventriculomm, and there is more frequently a
patency of the foetal communication between the auricles,
permitting the venous blood to pass into the arterial
system, and producing the livid appearance of the face
loiown as cyanosis.
The causes of congenital anomalies are di£Scult to specify.
There is no doubt that, in some cases, they are present in
the sperm or germ of the parent ; the same anomalies
recur in several children of a family, and it has been
found possible, through a variation of the circumstances,
to trace the influence in some cases to the father alone,
and in other cases to the mother alone. The remarkable
thing in this parental influence is that the malformation
in the child may not have been manifested in the body of
either parent, or in the grandparents. More often the
malformation is acquired by the embryo and fcetus in the
course of development and growth, either through the
mother or in itself independently. Maternal impressions
during pregnancy have often been alleged as a cause, and
this causation has been discussed at great length by the
best authorities. The general opinion seems to be that it
is impossible to set aside the influence of subjective states
of the mother altogether. The doctrine of maternal impres-
f ions has often been resorted to when any other explana-
tion was either difficult or inconvenient; thus, Hippocrates
is said to have saved the virtue of a woman who gave
birth to a black child by pointing out that there was a
picture of a negro on the wall of her chamber. Injuries
to the mother during pregnancy have been unquestion-
ably the cause of certain malformations, especially of
congenital hydrocephalus. The embryo itself and its
membranes may become the subject of inflammations,
atrophies, hypertrophies, and the like; this causation,
to which Otto traced all malformations of the foetus, is
doubtless accountable for a good many of them. But a
very large residue of malformations must still be referred
to no more definite cause than the erratic spontaneity of
the embryonic celb and cell-groups. The nisus formativus
of the fertilized ovum is always made subject to morpho-
logical laws, but, just as in extra-uterine life, there may
t c deviations from the beaten track ; and even a slight
<'eviation at an early ^tape will carry vi-ith it far-reaching I
consequences. This is particularly noticeable in donbU
monsters.
2. Double Monsters. — Twins are the physiological analogy
of double monsters, and some of the latter have come very
near to being two separate individuals. Triple monsters
are too rare to dwell upon, but their analogy would be
triplets. The Siamese twins, who died in 1874 at the
age of sixty, were joined only by a thick fleshy ligament
from the lower end of the breast-bone (xiphoid cartilage),
having the common navel on its lower border ; the anatom-
ical examination showed, however, that a process of peri-
toneum extended through the ligament from one abdominal
cavity to the other, and that the blood-vessels of the two
livers were in free communication across the same bridge.
There are one or two cases on record in which such a liga-
ment has been cut at birth, one, at least, of the twins
surviving. From the most intelligible form of double
monstrosity, like the Siamese twins, there m9 all grades
of fantastic fusion of two individuals into one down to
the truly marvellous condition of a small body or fragment
parasitic upon a well-grown infant, — the condition known
as fcettis in Joetu, These monstrosities are deviations, not
from the usual kind of twin gestation, but from a certain
rarer physiological type of dual development. In by far the
majority of cases twins have separate uterice appendages,
and have probably been developed from distinct ova ; but
in a small proportion of (recorded) cases there is evidence,
in the placental and enclosing stnicturea, that the twins
had been developed from two rudiments arising side by
side on a single blastoderm. It is to the latter physiological
category that double monsters almost certainly belong ;
and there is some direct embryological evidence for this
opinion. AQen Thomson observed in the blastoderm of a
hen's egg at the sixteenth or eighteenth hour of incubation
two " primitive traces " or rudiments of the backbone form-
ing side by side ; and in a goose's egg incubated five days ha
found on one blastoderm two embryos, each with the rudi-
ments of upper and lower extremities, crossing or cohering
in the region of the future neck, and with only one heart
between them. Somewhat similar observations had been
previously published (four cases in all) by Wolffi Von Baer,
and Beichert. Malformations in the earliest stages of the
blastoderm have been more frequently observed of late,
especially in the ova of the pike ; and these point not so
much to a symmetrical doubling of the primitive trace as to
irregular budding from the margin of the germinal disc. In'
any case, the perfect physiological type appears to be two
rudiments on one blastoderm, whose entirely separate de-
velopment produces twins (under their rarer circumstances),
whose nearly separate development produces such double
monsters as the Siamese tvrins, and whose less separate
development produces the various grotesque forms of two
individuals in one body. There can be no question of a
literal fusion of two embryos ; either the individuality of
each was at no time complete, or, if there were two dis-
tinct primitive traces, the uni-axial type was approximately
reverted to in the process of development, as in the forma-
tion of the abdominal and thoracic viscera, limbs,, pelvis, or
head. Double monsters are divided in the first instance
into those in which the doubling is symmetrical and equal
on the two sides, and those in which a small or fragment-
ary fcetus is attached to or enclosed in a fcetus of average
development, — the latter class being the so-called cases of
" parasitism."
Symmetrical Double Monsters are subdivided according
to the part or region of the body where the union or fusion
exists — head, thorax, umbilicus, or pelvis. One of the
simplest cases is a Janus head upon a single body, or there
maybe two pairs of ami:* with the two laces. Again, there
may be one head with two nec'is and two complete trunks.
766
M O N — M. O N
and pairs of extremities. Two distinct heads (witli moie
or less of neck) may surmount a singio trunk, broad at tho
shoulders but with onlj' one pair of arms. The fusion,
again, may be from the middle of the thorax downwards,
giving two heads and two pairs of shoulders and arms, but
only one trunk and one pair of legs. In another variety,
the body may be double down to tlie waist, but the pelvis
and lower limbs single. The degree of union in the region
of the head, abdomen, or pelvis may be so slight as to permit
of two distinct organs or sets of organs in the respective
cavities, or so great as to have the viscera in common ; and
there is hardly ever an intermediate condition between those
extremes. Thus, in the Janus head there may be two
brains, or only one brain. The Siamese twins are an instance
of union at the umbilical region, with the viscera distinct
in every respect except a alight vascular anastomosis and
a common process of peritoneum ; but it is more usual for
union in that region to be more extensive, and to entail a
single set of abdominal and thoracic viscera. The pelvis
is one of the commonest regions for double monsters to
be joined at, and, as in the head and abdomen, the
junction may be slight or tota.1. The Hungarian sisters
Helena and Judith (1701-1723) were joined at the sacrum,
but had the pelvic cavity and pelvic organs separate ; the
same condition obtained in the South Carolina negressea
MiUie and Christina, known as the " two-headed nightin-
gale," and in the other recent cs^e of the Bohemian sisters
Rosalie and Joaepha. More usually the union in the
pelvic region is complete, and produces the most fantastic
shapes of two trunks (each with head and arms) joining
below at various angles, and with three or four lower limbs
extending from the region of fusion, sometimes in a lateral
direction, sometimes downwards. A very curious kind of
double monster is produced by two otherwise distinct
foetuses joining at the crown of the head and keeping the
axis of their bodies in a Une. It is only in rare instances
that double monsters survive their bii'th, and the preserved
specimens of them are mostly of fretal si^e.
Unequal Double Monsters, Fastis, in. Foetu. — There are
some well-authenticated instances of this most curious of
all anomalies. The most celebrated of these parasite-
bearing monsters was a Genoese, Lazarus Johannes Baptista
Colloredo, bom in 1716, who was figured as a child by
Licetus, and again by Bartholinus at the age of twenty-
eight as a young man of average stature. The parasite
adhered to the lower end of his breast-bone, and was a
tolerably well-formed child, wanting only one leg; it
breathed, slept at intervals, and moved its body, but it
had no separate nutritive functions. The parasite is more
apt to be a miniatm'e acardiac and acephalous fragment,
as in the case of the one borne in front of ther abdomen
of a Chinaman figured by I. Geoffroy St-Hilaire. Some-
times the parasite is contained in a pouch under the skin
of the abdominal wall, and in another class (of which
there is a specimen in the Hunterian Museum) it has
actually been included, by tho closure of tho ventral laminre,
within the abdominal cavity of the foetus, — a true /cetus
mfortu. Shapeless parasitic fragments containing masses
of bone, cartilage, and other tissue are found also in tho
space behind the breast-bone (mediastinal teratoma), or
growing from the base of the skull and protruding through
tho mouth i'' epignathous teratoma," appearing to be seated
on the jaw), and, most frequently of all, attached to the
Rocrum. These last pass by a most interesting transition
into common forms of congenital sacral tumoiu-a (which,
may be of enormous size), consisting mainly of one kind
of tissue having its physiological typo in tho curious gland-
like body (coccygeal gland) in which the middle sacral artery
comes to an end. The congenital sacraJ tumours have a
tendency to become cystic, and thoy are probably related to
the more perfect congenital cysts of tho neck region, where
there is another minute gland-like body of the same nature
as the coccygeal at the point of bifurcation of the conunoi»
carotid artei-y. Other tumours of the body, especially
certain of the sarcomatous class, may be regarded from
the point of view of moiistra per excesswm ; but such cases
suggest not bo much a question of aberrant development
■n'ithin the blastoderm as of tho indwelling spontaneity of
a single post-embryonic tissue ; and they fall to be con-i
sidered more properly, along with tumours in general, ini
the article Pathology (q.v.).
The scientific appreciation of monsters hardly hegan before tho
18th century ; even so gi-eat a rationaUst in surgical practice as
Ambroise PariS (1617-1690), although he rtaa attracted as a echolitr
in later life to the subject, did not advance iu it uiateriaUy beyond
tlie fantastic and credulous staudpdint of the time, which is exems
plified in the elaborate treatise of Lycostheues, Pradigiorum ac oslen^
tonim ckroniccm, Basal, 1557. Throughout tlie 17th century fabulous
monsters continued to be described along v/ith actual specimens ;
the embryological studies of Harvey (1651) were doubtless calculated
to help iu the growth of rational opinion about monsters, though
Harvey himself mentions them only casually. The first syatematid
discussion of them from a strictly objective or anatomical point o2
view occurs in various writings of Haller from 1735 to 1753, and
the subject continued after that to engage a large amount of precLio
and philosophical thought on the part of Caspar Friedrich WolU
(1735-179'1), who first stated the relation of mgnatrosities to em^.
bryonic deviations in words that even now hardly requii-e to be
altered, and of^Blumenbach, Somrnering, Autenrieth, Tiedemann,
and others. The ongroaaing interest of the subject in the early
part of the 19th century is shown by the fact that. J. P. Meckel a
Bandhuch der -patkolojischen Aiuximnie (1817) was largely occupied
with congenital malformationa. Geofiroy St-HiJaire, the father,
gave them a prominent place in his Philosophie Anat(ymique (Pans,
1822), and his son Isidore made them the subject of a special and
very elaborate » treatise in 3 vols. (Paris, 1832-37), illustrated by a
small and iuade<|uate atlas of plates. Monstrosities were at this
period a prominent part of all test-books of morbid anatomy. Fronx
1840 to 1850 may be regarded as the period in which human tera-
tology reached its highest point ; in 1810-42 the special tieatise of
Vrolik was published (2 vols., Amsterdam), containing an introduc-
tion on the normal development, and Ids sumptuous and incompar-
able atlas to the same followed in 1849 ; iu 1841 Otto published at
Warsaw a description of 600 monatora with 30 folio platea ; and in
1842 the embryologist Bischofl" conti-ibuted to "Wagner's Handwort-
erbuch der Physiologie, voL L, an article on teratology as elucidated
by the best information on mammalian development An article
by Allen Thomson in the London and Edinhurgh Monthly Journal
of Medical Scit^ice, July 1844, followed by a criticai survey in tho
next number, is of the first impoi-tance for the theory of double
monsters, and it is one of the few notable Enghsb contributions to
animal teratologyapart from museum catalogues, — thegenerai article
in Todd's Cycl&pmdia of A natomy and Pkysioloijy having been written
by Vrolik, while the special subject of Hermaphroditism is treated
of in a long and learned article by J. Y. Simpson (reprinted in his
collected works). One of the latest important works on moustera
is that by Forster (Jena, 1861), I)ic Misihildungen dcs Mensdicn
systcmalisch dargcstclU, with an atlas of 2ti 4 to phtes containing
624 figures (on a small scale), of which 162 were drau-n from original
specimens, mostly in tho Wiirzburg Museum ; this work has a very
great variety of illustrations from all som'ces, and most copious
bibliographical references. The newest treatise is Ahlfeld's Mus-
hildungen dcs Mcnscheti (Leipsic, 1880-82), with an extensive atlas
of folio platea, aa comprehensive aa Forster's and on a larger scale.
Monsters have of late been assigned a comparatively subordinate
position in pathological teaching, owing, doubtless, to the more im-
mediate interest of microscopic and experimental patholo[;y. Among
recent pathological text-books that of Perls (Stuttgart, 1877-79)
may bo named as containing an adequate treatment of the subieot.
The two most considerable contributors to teratology recently have
been Panum (Doriin, 1860), and Darcste (Paris, 1877), both of whom
have occupied themselves mainly with producing monstrosities arti-
ficially in the bird's egg by varying the temperature in the hatching
oven. See also L. Gerlach, Z)ie E?itst<hungsjc< ise der Doppclmissbit-
dungen bei dtn h>Hcmi Wirlclthicrcn, Stuttgart, 188S. (C. C.)
MONSTRELET, ENcmiKKAiCT) de (oi. 1453) (who,
rather owing to accident than to merit, held, until within
the present century, the same position as chronicler of
French affairs during the early part of the ir>th century
OS Froissart deservedly holds with regard to the last half
of the 14th), was bom at an uncertain date, apparently
not Inter than 1400, a»d die! in July 14.')3. He was ol
jtt.P 1^;— -^ 0 N
767
k nobie family in the district of Bonlogne. He held in
U36. and '.ater, the office of lieutenant-gavenier (receiver
of the -/us.'e, a kind of ciiuich rate) in the city of Cambray,
and seems to have usually resided there. : Besides this he
,«ras for somo time baUifif of the chapter of that city, and
later provost. He was married, and left children. But
this- ahnost exhausts the amount of our knowledge respect-
ing him, except that he was present, not at the capture of
the Maid of Orleans, but at her svibsequent interview with
'the duke of Burgundy. As a subject of this latter prince
he naturally takes the Burgundian side in his history, which
extends in the genuine part of it to two books, and covers
the period from 1400 to Uii. At this time, as another
chronicler Matthieu de Coucy informs us, Monstrelet ceased
writing. But, according to a habit by no means uncommon
in the Middle Ages, a clumsy sequel, extending to a period
long subsequent to his death, was formed out of various
other chronicles and tacked on to his work. The genuine
part of this, dealing with the last half of the Hundred Years
War, is valuable because it contains a large number of
documents which are certainly, and reported speeches which
are probably, authentic. It has, however, little colour or
narrative merit, is dully, though clearly enough, written,
and is strongly tinged with the pedantry of its century, —
the most pedantic in French history. The best edition is
that published for the Soci^t6 de I'Histoire de France by
M. Douet d'Arcq in 1856.
MONTAGU, Lady Maky Woetley (1690-1762), one
of the most brilliant letter- wTiters of the 18th century, was
the eldest daughter of Evelyn Pierrepont, duke of Kingston,
and Lady Mary Fielding, daughter of the earl of Denbigh.
Her near relationship with Fielding the novelist is worth
remarking. She was bom at Thoresby in Nottingham-
shire in 1690. Her mother died when she was a child,
and by some chance she received or gave herself an un-
usually wide literary education, had the run of her father's
library, was encouraged in her studies by Bishop Burnet,
and while still a girl translated the Enchiridion of Epic-
tetus. After a courtship in which she showed a singular
power of thinking for herself, she was married in 1712,
against her father's wish, to Mr. E. Wortley Montagu,
an accomplished and scholarly friend of the Queen Anne
wits. At the new court of George I. her beauty and
wit brought her much homage ; Pope was among her
most devoted worshippers, and she even gained and kept
the friendship of the great duchess of Marlborough. Her
husband being appointed ambassador to the Porte in
1716, she accompanied him to Constantinople, and wTote
to her friends at home brilliant descriptions of Eastern life
and scenery. These letters were not published till 1763,
!the year after her death ; but, copies being handed about
in fashionable circles, their lively, witty style, graphic
pictures of unfamiliar life, and shrewd and daring judg-
ments gave the writer instant celebrity. In one of them
she described the practice of inoculation for the smallpox,
and announced her intention of trying it on her own son,
and of introducing it in spite of the doctors into England.
The most memorable incident in her life after her return
from the East was her quarrel with Pope, caused, accord-
ing to her account, by her laughing at him when he made
love to her in earnest. He satirized her under the name
of Sappho, and she teased him with superior ingenuity
and hardly inferior wit. From 1739 to 1761 Lady Mary
lived abroad, apart from her husband, maintaining an
iffectionate correspondence with her daughter Lady Bute,
in , which she set forth views of life largely coloured by
tthe asceticism of her master Epictetus, and wearing an
jfeppeaftmcs of oddity and eccentricity from their contrast
jtvith conventional thought. The character of coldness
and un womanliness whici^ Pope contrived to fasten on his
enemy was far from being desei .cu ; uer letters show her
to have been a very warm-hearted w(}man, though on
principle she turned the hard side to the world. She
died 21st August 1762. The best edition of her works is
that of 1861, with a memoir by Moy Thomas.
MONTAIGNE, Michel de (1533-1592), essayist, was
born, as he himself tells us, between eleven o'clock and noon
on 28th February 1533. The patronymic of the Montaigne
family, who derived their title from the chateau at which
the essayist was born and which had been bought by his
grandfather, was Eyquem. It was believed to be of Eng-
lish origin, and the long tenure of Gascony and Guienne by
the English certainly provided abundant opportunity for the
introduction of English colonists. But the elaborate re-
searches of M. Malvezin have proved the existence of a
family of Eyquems or Ayquems before the marriage of
Eleanor of Aquitaine to Henry II. of England, though
no connexion between this family, who were Sieurs do
Lesparre, M..id the essayist's ancestors can be made out.
Montaigne is not far from Bordeaux, and in Montaigne's
time was in the province of Perigord. It is now in
the arrondis'sement of Bergerac and the department of
Dordogne. The Eyquem family had for some time been
connected with Bordeaux. Indeed, though they possessed
more than one estate in the district, they were of doubt-
ful and certainly very recent nobility. Pierre Eyquem,
Montaigne's father, had been engaged in commerce (a
herring-merchant Scaliger calls him), had filled many
municipal offices in Bordeaux, and had served under
Francis I. in Italy as a soldier. The essayist was not
the eldest son, but the third. By the death of his
elder brothers, however, he became head of the family.
He had also six younger brothers and sisters. His father
appears, like many other men of the time, to have made
a hobby of education. Michel was not a strong boy,
indeed he was all his life a valetudinarian, and this may
have esiiecially prompted his father to take pains with
him. At a time when the rod was the universal instru-
ment of teaching it was almost entirely spared to
Montaigne. He was, according to the French fashion
common at all times, put out to nurse with a peasant
woman. But Pierre Eyquem added to this the unusual
fancy of choosing his son's sponsors from the same class,
and of accustoming him to associate with it. He was
taught Latin orally by servants who could speak no French,
and many curious fancies were tried on him, as, for
instance, that of waking him every morning by soft music.
But he was by no means allowed to be idle. A plan of
teaching him Greek, still more out of the common way
than his Latin course, by some kind of mechanical
arrangement, is not, very intelligible, and was quite un-
successful. These detaUs of his education (which, like
most else that is known about him, come from his own
mouth) are not only interesting in themselves, but remind
the reader how, not far from the same time, the other
greatest writer of French during the Renaissance was also
exercising himself, though not being exercised, in plans of
education almost as fantastic. At six years oM (for the
father's reforming views in education do not seem to have
disgusted him ^Wth the extremely early age at which it
was then usual to begin school training) Montaigne was
sent to the College tic Guienne at Bordeaux, then at the
height of its reputation, having more than double the
number of scholars (two thousand) that even the largest
English public school has usually boasted. Among its
masters were Buchanan, afterwards the teacher of James
I., and MuretuE, one of the first scholars of the age. These,
vrith their colleague Gu^rente, composed Latin playa for
their pupils to act, and are held to have given no smalS
imDulse to the production of the classical French tragedy
768
MONTAIGNE
■of the Tliiade. Montaigne remained at school aeveu years,
and, lite almost all Frenchmen of all fim^s, retained no
pleasant or complimentary memory of it. At thirteen he
left the College de Guienne and began to study law, it is
r.ot known where, but probably at Toulouse, the most
famous university, despite its religious intolerance, of the
EDuth of France. Of his youth, early manhood, and middle
life extremely little is known. Allusions to it in the
Essays are frequent enough, but they are rarely precise.
In 1548 ho was at Bordeaux during one of the frequent
riots caused by the gabeUe, or salt tax. Six years afterwards,
having attained his majority, he was made a counsellor in
ithe Bordeaux parliament. In 1558 he was present at the
siege of ThionvUle. Like his father, he certainly served
in the army, for he has frequent allusions to military
experiences. He was also much about the court, and
be admits very frankly that in his youth he led a life of
pleasure, if not exactly of excess. In 1566 he married
Fran^oise de la Chassaigne, whose father was, like himself,
a member of the Bordeaux parliament. Three years later
1 is father died, and he succeeded to the family possessions.
Finally, in 1571, as he teUs us in an inscription still extant,
he retired to Montaigne to take up his abode there. This
was the turning-point of his life.
It has been said that his health was never strong, and
it had been further weakened by the hard living (in both
censes of that phrase) which was usual at the time. He
resolved, accordingly, to retire to a life of study and con-
templation, though he did not in the least seclude himself,
and indulged in no asceticism except careful diet. Mon-
taigne was a large country house unfortified (in which
circumstance its astute possessor saw rather safety, than
danger from the turbulence of the religious wars), and its
owner's revenues, without being large, appear to have been
easy. He neither had nor professed any enthusiastic
affection for his wife, but he lived on excellent terms with
her, and bestowed some pains on the education of the orJy
child (a daughter) who survived infancy. In his study,
■which he has minutely described, he read, wrote, dictated,
tneditated, inscribed moral sentences, which still remain on
the walls and rafters, and in other ways gave himself up
to learned ease. He was not new to literature. In his
father's lifetime, and at his request, he had translated the
Wheologia Naturalis of Raymond de Sebonde, a Spanish
schoolman. On fij-st coming to live at Montaigne he
edited the works of his deceased friend iltienne de la
iBo^tie, who had been the comrade of his youth, who died
early, and who, with poems of real promise, had composed
B declamatory and schoolboyish theme on republicanism,
entitled the Contr' Un, which is one of the most over-
estimated books in literatirre. But the years of his
studious retirement were spent on a work of infinitely
greater importance. Garrulous after a fashion, as Mon-
taigne is, he gives us no clear idea of any original or
definite impulse leading him to write the famous Essays.
It is very probable that if they were at first intended to
have any special form at all it was that of a table-book
or journal, such as was never more commonly kept than
in the 16ih century. But the author must have been
more or less conscious of an order existing in the disorder
of his thoughts, and this may have induced him to keep
them apart in chapters, or at Ici-st under chapter-headings,
and at the same time not to cut them up into mere 2i^i''sces.
It is certainly very noticeable that the earlier essays, those
of the first two books, differ from the later in one most
striking point, in that of length. Speaking generally, the
essays of the third book aver.age fully four times the
length of those of the other two. This of itself would
suggest a difference in the system of composition. For
the present, however, we may confine oiu-selves to the first
two books. These appeared in 1580, when their author
was forty-seven yearn old
Thoy contain, as at T-escnt published, no less than ninety-thr6«
essays, besides an cxcieiiiagly long apology for the already-men-
tioned Raymond Sebonde, which amounts to about a quarter of the
whole in bulk, and dilTers ciniously from its companions in matter
no less than in scale. The book bemns with a snort avis (address
to the reader), opening with the well-known words, " C'est icy un
livre de bon foy lecteur, " and sketching in a few lively sentencoa
the character of meditative egotism which is kept up throughout.
His sole object, the author says, is to leave for his friends and
relations a mental portrait of himself, defects and all ; he cares
neither for utility nor fame. The essays then begin ■n'ithout any
attempt to explain or classify their subjects. Their titles are of the
most diverse character. Sometimes they are proverbial sayings, or
moral adages, such as: " Par divers moyens on arrive ^ pareille fin",
**Qu'il ue faut juger de notre heur qu'apPL'S la mort", "Le profit de
Ton est le dommage de I'aultre. " Sometimes they are headed like the
chapters of a treatise on ethics : ** De la tristesse ", * ' De I'oisivet^ ",
"De la peur", "De I'amitid." Sometimes a fact of some sort
which has awaked a train of associations in the mind of the writer
serves as a title, such as: " On est puni de ^'opiniastrer h. une place
sans raison ", " De la bataille de Dreux ", &c. Occasionally the titiM
seem to be deliberately fantastic, as : " Des puces ", " De I'usage de
se vestir. " Sometimes, though not very often, the sections are in no
proper sense essays, but merely commonplace book entries of singular
facts or quotations with hardly any comment. These point to
the haphazard or indirect origin of them which has been already
suggested. But generally the essay-character — that is to say, the
discussion of a special point, it may be with wide digressions and
divergences — displays itself. The digressions are indeed constant,
and sometimes have the appearance of being absolutely wilful.
The nominal title, even when most strictly observed, is rarely more
than a starting-point ; and, though the brevity of these first essays
for the most part prevents the author from journeying very far, he
contrives to get to the utmost range of his tether. Quotations are
very frequent. These are the principal external characteristics of
the book ; its internal spirit had better bo treated when it can bo
spoken of completely.
Between the publication of the first two books of essays
in 1580 and the publication of the third in 1588, Mon-
taigne's life as distinguished from his writings becomes
somewhat better known, and somewhat more interesting.
He had, during the eight years of composition of his first
volume, visited Paris occasionally and travelled for health
or pleasure to Cauterets, Eaux Chaudes, and elsewhere.
Charles IX., apparently, had made him one of his gentle-
men in ordinary, and perhaps conferred on him the order
of St Michael. The fiercest period of the religious wars,
save that yet to come of the League, passed over him with-
out harming him, though not without subjecting him to
some risks. But his health grew worse and worse, and he
was tormented by stone and gravel. He accordingly re-
solved to journey to the baths of Lucca. Late in Ae 18th
century a journal was found in the chateau of Montaigne,
giving an account of this journey, and it was published in
1774; par-t of it is -written in Italian and part dictated
in French, the latter being for the mo.st part the work
of a secretary or servant. Whatever may be the biographi-
cal value of this work, which has rarely been reprinted
with the Essays themselves, it is almost entirely destitute
of literary interest. Written, moreover, according to its
own showing merely for the author's own eye, it contains
abundance of details as to the medicinal effect of the
various baths which he visited, details which may be said
to be superfluous to a medical reader, and disgusting to
any other. The course of the journey was first north-
wards to Plombicres, then by Basel to Augsburg and
Munich, then through Tyrol to Verona and Padua in Italy.
Montaigne -visited most of the famous cities of the north
and centre, staying five months at Rome, and finally
establishmg himself at the baths of Lucca for nearly as
Ion" a time. There he received news of his election as
mayor of Bordeaux, and after some time journeyed home-
wards. The tour contains much minute information about
roads, food, travelling, i'C, but the singidar ^condition in
which it exists, and the absence of a really good critical
MOKTAIGNE
'6'9
edition liitherto, make it rather difficult to use it as a
document. The freak of writing part of it in a strange
dog-Italian is not uncharacteristic of Montaigne, but the
words of his last and best editors, MM. Courbet and
Royer, who speak of the letters as " I'unique complement
des essais," seem to indicate that they are not of those
who accept the published Voyage as authentic. Of the
fact of the journey there is no doubt whatever.
Montaigne (as was not unnatural in a man of his tempera-
ment, who had for some years, if not for the greater part
of his life, lived solely to please himself) was not altogether
delighted at his election to the mayoralty, which promised
him two years of responsible if not very hard work. The
memory of his father, however, and the commands of the
king, which seem to have been expressed in a manner rather
stronger than a mere formal confirmation, induced him to
accept it ; and he seems to have discharged it neither better
nor worse Ihan an average magistrate. Indeed, he gave
sufficient satisfaction to the citizens to be re-elected at the
close of his term, and it may be suspected that the honour
of the position, which was really one of considerable dignity
and importance, was not altogether indifferent to him.
Unfortunately, it cannot be said that nothing in his office
became Viim like the leaving of it, for it was at the close
of his second tenure that he gave the only sign of the
demoralizing effect which is sometimes alleged by severe
moralists to come of the half epicurean, half sceptical philo-
sophy which he imdoubtedly professed. It was his business,
if not exactly, his duty, to preside at the formal election of
his successor, the marechal de Matignon ; but there was a
severe pestilence in Bordeaux, and Montaigne writes to the
jurats of that town, in one of the few undoubtedly authentic
letters which "we possess, to the effect that he will leave
them to judge whether his presence at the election is so
necessary as to make it worth his while to expose himself
to the danger of going into the town in its then condition,
" which is specially dangerous for men coming from a good
air as he does." That is to say, the chief magistrate of one
of the greatest towns in France not only declined to visit
it because of sickness prevailing there, but had left it to
itself at a time when nearly half the population perished,
and when, according to the manners of the age, civil dis-
turbance was almost sure to follow accordingly. Attempts
have been made to justify Montaigne, and it may be at
least said that he at no time pretended to unselfish heroism ;
but it is to be feared that the facts and the inference drawn
from them admit of no dispute. At the least, Montaigne's
conduct must be allowed to contrast very little to his
advantage with that of Eotrou in the next century under
somewhat similar circumstances though in a position of
much less responsibility. It may, however, be urged in
Montaigne's favour that the general circumstances of the
time, where they did not produce reckless and foolhardy
daring, almost necessarily produced a somewhat excessive
caution. The League was on the point of attaining its
greatest power; the extreme Calvinist and Navarrese party,
on the other side, was (as may be seen in Agrippa d'Aubign^)
no less fanatical than the League itself, and the salvation
of France seemed to lie in the third party of politiques, or
trimmers, to which Montaigne belonged. The capital
motto of this party was that of the Scotch saying, " Jouk
and let the jaw gang by," and the continual habit of parry-
ing and avoiding political dangers might be apt to extend
itself to dangers other than political However this may
be, Montaigne had difficulty enough during this turbulent
period, all the more so from his neighbourhood to the chief
haunts and possessions of Henry of Navarre. He was
able, however, despite the occupations of his journey, his
mayoralty, and the pressure of civil war and pestilence,
which was not confined to the town, to ' continue his essay
writing, and In 1588, after a TOit of some length to Paris,
the third book of the Essays was published, together with
the former ones considerably revised. The new essays, aa
has been remarked, differ strikingly from the older ones in
respect of length ; there being only one which confines
itself to the average of those in the first two books. The
whimsical unexpectedness of the titles, moreover, reappears
in but two of them : " Des coches " and " Des boiteux.*
They are, however, identical with the earlier ones in spirit,
and make with them a harmonious whole — a book which'
has hardly been second in influence to any of the modem
world.
This influence is almost equally remarkable in point of mattei
and in point of form, as regaras the subsequent history of thought
and as regards the subsequent history of literature. The latter aspect
may be taken first. Montaigne is one of the few great writers whc
have not only perfected but have also invented a literary form.
The essay as he gave it had no forerunner in modern literature, and
no direct ancestor in the literature of classical times. It is indeed
not improbable that it owes something to the body of tractates by
different a? '* -rs and of different dates, which goes under the name
of Plutarch's Morals, and it also bears some resemblance to the
miscellaneous work of Lucian. But the resemblance is in both cased
at most that of ^suggestion. The peculiar desultoriness and tenta-
tive character of the essay proper were alien to the orderly character
of the Greek mind, as were also its garrulity and the tendency which
it has rather to reveal the idiosyncrasy of the writer than to deal in
a systematic manner with the peculiarities of the subject. It has
been suggested that the foi-m which the essays assumed was in a
way accidental, and this of itself precludes the idea of a definite
model even if such a model could be found. Beginning with the
throwing together of a few stray thoughts and quotations linked
by a community of subject, the author by degrees acquires more
and more certainty of hand, until he produces such masterpieces of
apparent desultoriness and real imity as the essay " Sur des vers da
Virgile." In matter of style and language Montaigne's position is
equally important, but the ways winch led him to it are mor«
clearly traceable. His favourite author was beyond all doubt Plu-
tarch, and his own explicit confession makes it undeniable that
Plutarch's translator Ainyot was his master in point of vocabulary,
and (so far as he took any lessons in it) of style. Amyot was
unquestionably one of the most remarkable writers of French in
the 16th century, and to him more than to any one else is due
the beauty of the prose style which marked the second half of
that century, a style which, though unequal and requiring to b«
modified for general use, is at its best the very flower of the lan-
guage. Montaigne, however, followed with the perfect independence
that characteri2ed him. He was a contemporary of Konsard, and
his first essays were published when the innovations of the Pleiade
had fully established themselves. He adopted them to a great
extent, but with much discrimination, and ne used his own judg-
ment in Latinizing when he pleased. In the same way he retained
archaic and provincial words with a good deal of freedom, but by
no means to excesa In the aixan^ment as in the selection of hia
language he is equally original. There is little or no trace in him
of the interminable sentence which is the drawback of early prose
in all languages when it has to deal with anj-thing more difficult
to manage than mere narrative. He has not the excessive classicism
of style which mars even the fine prose of Calvin, and which makes
that of some of Calvin's followers intolerably stiff. As a rule he is
careless of definitely rhythmical cadence, though his sentences are
always pleasant to the ear. But the principal characteristic of
Montaigne's prose style is its remarkable ease and flexibility. 'These
peculiarities, calculated in themselves to exercise a salutary influ-
ence on a language as yet somewhat undisciplined, acquired by
accident an importance of an extraordinary kind. A few years
after Montaigne's death a great revolution, as is generally known,
passed over French. The criticism of Malherbe, followed by the
establishment of the Academy, the minute grammatical censures of
Vaugelas, nnd the severe literary censorship of Boileau turned
French in less than three-quarters of a century f'.om one of the
freest languages in Europe to one of the most restricted. The
Latinisms and Gnecisms of the Pleiade were tabooed at the same
time with the most picturesque expressions of the older tongue.
The efforts of the refoi-mers were directed above all things to weed
and to refine, to impose addirional difficulties in the way of writing
exquisitelv, at the same time that, by holding out a strictly-defined
model, they assisted persons of little genius and imagination to
write tolerably. During this revolution only two WTitci-s of older
date held their ground, and those two were Kabclais and Montaigne,—
Montaigne being of his nature more generally readable than Rabe-
lais. The Essaijs, the popularity of which no academic censorship
could touch, thus kept beforj the eyes of the ITth and 18th '■c;i-
turies a treasury of French in which every generation cculd behold
XVI. — 97
770
MONTAIGNE
the riclies cl tbrir ancfif^tors.- The study cf them influenced all the
great pros? writorfl of France, and they could not fail to bo influ-
enced in the di" ^i^tion which it was moat important that they should
take by the racy phi-ase, the quaint and picturesque vocabulary,
and the unconstrained constructions of Montaigne.
It would be in-.possible, however, for the stoutest defender of the
importance of form in literature to assign tho chief part in Mon-
taigne's influence to style. It is the method or rather the manner
of thinking of which that style is the garment which has in reality
exercised influence on the world. Like all writers except Shake-
speare, Montaigne thoroughly and completely exhibit's the intellec-
tual and moral complexion of his own time. When he reached man-
hood the French. Renaissance (which was perhaps on the whole the
.most characteristic example of that phenomenon, the religious
element being neither in excess as it was in England and Germany,
nor in defect as it had been in Italy) was "at high water, and the turn
of the tide was beginning. Rabelais, who died when Montaigne was
still in early mannood, exhibits the earlier and rising spiiit, though
he needs to be completed on the poetical side. 1 he Renaissance
had, as all revolts against "authority must have, a certain sceptical
element, but it was not at first by any meana eminently sceptical.
Despite the hali' ironical, half warning termination of Pardagriiely
an immense confidence snd delight, as of the invader of a promised
land, fills the pages of Rabelais. He rejoices in his strength, in his
knowledge, in his freedom, in the pleasures of the flesh and the spirit.
With Montaigne begins the age of disenchantment. By the time
at least when he began to meditate his essays in the retirement of
bis country house it was tolerably certain that no golden age- was
about to return. The Reformation had brought not peace but a
sword, and the Calvinists were as intolerant as the Catholics. The
revival of learning had, whatever its. benefits, merely changed the
outward guise of pedants instead of extirpating pedantrj'. The
art of printing had multiplied rubbish as well as valuable matter.
The discovery of America had brought ruin to the discovered, and
disease and discord to the discoverei-s. The horrors of a disputed
succession were already threatening Franco. These things were
enough to make thoughtful meu dubious about the blessings of
progress and reform ; but the extreme dissoluteness which charac-
terized the private life of the time also brought about its nati'ral
result of satiety. Physical science had hardly yet emerged to occupy
some active minds ; scholasticism was dead, while Bacon and Des-
cartes had not arisen ; nothing like a theory of politics had been
evolved, though Bodin and a few others were feeling after one. As
Ihe earlier Renaissance had specially occupied itself Avith the prac-
tical business and pleasures of life, so the later Renaissance specially
mused on the vanity of this business and these pleasures. The pre-
disposing circumstances which afl"ected Montaigne were thus likely
to incline him to sceptiL-ism, to ethical masings on the vanity of life
and the like. But to all this there had to be added the peculiarity
of his own temperament This was a decidedly complicated one,
and neglect of it has led some readers to adopt a more positive idea
of Montaigne's scepticism than is fully justified by all the facts. The
municipality of Rome has put up a tablet on the house occupied
by Montaigne during his visit there, which speaks of him as a
"founder of the new philosophy." In Italian mouths, at the
present day this is equivalent to an assertion that Montaigne was
aa enemy of Christianity. No assumption can be more gratuitous
or less borne out by the text of his works and the reasonable
iuferences to be drawn from them. The attitude which he assumed
v.aa no doubt ephectic and critical chiefly. He decorated his study
at; Montaigne with inscriptions (still, by dint of accidental
pi-eservation and restoration not accidental, legible there), most of
which are of the most pessimist and sceptical character. Eccle-
uiostes, Ecclesiasticus, Horace, Lucretius, Sextus Empiricus, the
fragments of the Greek dramatists and philosophers, are ransacked
f>fr epigraphs indicating the vanity of human reason, human wishes,
humati belief, human thoughts and actions of every kind. In ouo
I'urious essay (if indeed it is to be called an essay), the '* Apologie
de Raymond Sebondo," he has apparently amused himself with
•gathering together, in the shape of quotations as well as of re-
flexions, all that can bo said against certainty in aesthetics as well as
in dogmatics. But the general tenor of the essays is in complete
contrast with this sceptical attitude, at least in its more decided
form, and it is worth notice that the motto *' Que scai-je ? " does not
appear on the title page till after tho writer's death. The general
disposition, moreover, manifested in these famous writings is very
far from being determinedly Pyrrbonist or despairingly misanthro-
pic. Montaigne is far too much occupied about all sorts of the
minutest details of human life to make it for a moment admissible
that he regarded that life as a whole but as smoke and vapour.
He is much too curious of the varieties of belief, and too keenly
interested in following them out, to leave himself in peril of the
charge that all belief was to him a matter of indifference. The
reason of the misapprehension of him which is current is due very
mainly to the fact tnat he was eminently a humorist in the midst
•f a pcopio to whom, since his time, humour has been nearly un-
Imown. But thei« is more than this. The humorist u« a recog-
nized gcna^ almo<jt always passes into the liatiriflt. The temped
which nas been admirably defined as thinking in jest while feehng
in earnest uatuially throws itself into opposition, though it may
not always take the irreconcilable form ot the opposition of Swift
Perhaps the only actual parallel to Montaigne in literature is Lamb.
There are differences between them, arising naturally enough
from differences of temperament and experience ; but both agree
in their attitude — an attitude which is sceptical without being
negctive, and humorist without being satiric There is hardly any
writer in whom the human comedy appears treated with such
completeness as it is in Montaigne. There is disconiible in his
essays no attempt to map out a complete plan, aud then to fill
up its ouUines. But in the desultory and haphazard fashion
which distinguishes him there are few parts of life on which he
does not touch. The exceptions are chiefly to he found in tho
higher and more poetical strains of feeling to which the humorist
temperament lends itself \vith reluctance and distrust, though it
by no means excludes them. The French disposition, by a change
which has never been sulficiently accounted for, and of which the
mpst accurate examination of documents fails fully to detect the
reason, had become, after being strongly idealist in the earlier Middle
Ages,, absolutely positive in the later, and from this positiveness it
has never since quite freed itself. This positiveness is already notice-
able in Rabelais ; it becomes more noticeable still in Montaigne. Ho
is always charming, but he is rarely inspiring, except in a very few
passages where the sense of vanity and nothingness possesses him
with unusual strength. As a general rule, an agreeable grotesque
of the affairs of life (a gi-otesque which never loses hold of good
taste Eufticiently to bo called burlesque) occupies him. Theie is a
kind of anticipation of the scientific spirit in the careful zeal with
which he picks up odd aspects of mankind, and comments upon
them as he places them in his museum. Such a temperament is
most pleasautly shov/n when it is least personaL The letter to
the Bordeaux jurats does not, as has been said, show Montaigne
in his best light, nor does another letter to his wife, in which
he condoles with her on the death of one of their childi-en in a
strain which must have drawn from any woman of sensibility and
spirit a torrent of indignant tears. But what is almost ofl"ensive
in immediate and private relationships becomes not only toler-
able but delightful in the impersonal and in'esponsible relationship
of author to reader. A dozen generations of men have rejoiced in
the gentle irony with which Montaigne handles the ludicrum hu-
ma}ii ssccidi^ in the quaint felicity of his selection of examples, and
in the real though sometimes fUntastic wisdom of his comment on
hia selections,
Montaigne did not very long survive the completion of
his book. His sojourn at Paris for the purpose of getting
it printed was by no means uneventful, and on his way lie
'stayed for some time at Blois, where he met De Thou. lu
Paris itself he had a more disagreeable experience, being
for a short time committed to the Bastille by the Leaguers,
as a kind of hostage, it is said, for a member of their party
who had been -arrested at Rouen by Heniy of Navarre.
But he was in no real danger. He was well known to
and favoured by both Catherine de' Medici and the Guises,
and was very soon released. In Paris, too, at this time he
made a whimsical but pleasant friendship. Marie le Jars,
Demoiselle de Grournay, one of the most learned ladies of
the 16th and 17th centuries, had conceived such a venera-
tion for the author of the Essays that, though a very
young girl and connected with many noble families, she
travelled to the capital on purpose to make his acquaint-
ance. Ho gave her the title of his "fille dalliance"
(adopted daughter), which she bore proudly for the rest
of her long life. She lived far into the 17th century, and
became a character and something of a laughing-stock to
the new generation; but her services to Montaigne's literary
memory were, as will be seen, great. Of his other friends
in these last years of his life the most important were
fitienne Pasquicr and Pierre Charron. The latter, indeed,
was more than a friend, he was a disciple ; and Montaigne,
just as he had constituted Mademoiselle de Goumay his
*' fiUe d'alliance," bestowed on Charron the rather curious
compliment of desiring that 'he should take the arms of the
family of Montaigne. It has been thought from these two
facts, and from an expression in one of the later essays,
that the marriage of his daughter L6onore had not turned
out to his satisfaction. But family affection, except towards
his futiier, w&s by no meaiia Montaigne's etropgest point.
M O N — M O N
771
"Not much is known of liim in tl\ese later years, and
indeed, despite the laborious researches of many bio-
graphers, of whom one, Dr Payen, has never been excelled
in persevering devotion, it cannot be said that the
amount of available information about Montaigne Is large
at any time of his life. It would seem that the essayist
had returned to his old Ufe of study and meditation
and working up his Essays. No new ones were found
after his death, but many alterations and insertions. Els
various maladies grew worse ; yet they were not the direct
cause of his death. He was attacked with quinsy, which
rapidly brought about paralysis of the tongue, and he died
on the 11th of September 1592, under circumstances which,
as Tasquier reports them, completely disprove any intention,
at least on his part, of displa)'ing anti-Christian or anti-
Catholic leanings. Feeling himself on the point of death,
he summoned divers of his friends and neighbours to his
chamber, had mass said before him, and endeavoured to
raise himself and assume a devotional attitude at the
elevation of the host, dying almost immediately afterwards.
He was buried, though not till some months after his
death, in a church in Bordeaux, which after some vicissi-
tudes became the chapel of the College. During the
Eevolution the tomb and, as it was supposed, the coffin
were transferred with much pomp to the town museum ;
but it was discovered that the wrong coffin had been taken,
and the whole was afterwards restored to its old position.
Montaigne's widow survived him, and his daughter left pos-
terity which became merged in the noble houses of S^gur
and Lur-Saluces. But it does not appear that any male
representative of the family survived, and the chateau is
not now in the possession of any descendant of it.
"When Mademoiselle de Goumay heard of the death of Mon-
taigne she undertook with her mother a visit of ceremony and con-
dolence to the widow, which had important results for literature.
Madame de Montaigne gave her a copy of the edition of 158S,
Annotated copiously ; at the same time, apparently, she bestowed
another copy, also annotated by the author, on the convent of the
Feuillants in Bordeaux, to which the church in which his remains
lay was attached. Mademoiselle de Goumay thereupon set to work
to produce a new and final edition with a zeal and energy which
would have done credit to any editor of any date. She herself
worked with her own copy, inserting the additions, marking the
alterations, and translating all the quotations. But when she had
got this to press she sent the proofs to Bordeaux, where a poet of
some note, Pierre de Brach, revised them \vith the other annotated
copy. The edition thus produced has with justice passed as the
standard even in preference to those which appeared in the author's
lifetime. Unluckily, Mademoiselle de Gournay's original does not
appear to exist, and her text was said, until the appearance of MM.
Courbet and Royer's edition, to have been somewhat wantonly
corrupted, especially in the important point of spelling. The
Feuillants copy is in existence, being the only manuscript or partly
manuscript authority for the text. It was edited in 1803 by
Naigeon, the disciple of Diderot ; but, according to later inquiries,
considerable liberties were taken with it. The fS-st edition of 1E80,
with the various readings of two others which appeared during the
author's lifetime, was reprinted by MM. Dezeimeris and Burck-
htusen. Hitherto the edition of Lo CTerc {3 vols., Paris, 1826-28)
and in a more compact form that of Louandre (1 vols., Paris, 1854)
have been the most usefuL The edition, however, of MM. Courbet
and Royer, which ia based on that of 1595, will undoubtedly be the
titandard ; but, though the text is complete (Paris, Lemerre, 1873-
1877), the fifth volume, containing the biography and all the editorial
apparatus, has unluckily yet (1883) to make its appearance. The
editions of Montaigne in France and elsewhere, and the works upon
him during the past three centuries, are innumerable. His influence
upon his successora has already been hinted at, and cannot here
be traced in detail. In one case, however, — that of Pascal — it is of
sufficient importance to deserve mention. Pascal, who has left a
special discourse on Montaigne, was evidently profoundly influenced
by him, and the attitude towards his teacher is an interesting one.
The sceptical method of the essayist is at once tempting and terrible
to him. He accepts it in so far as it demolishes the 'claims of
human reason and heathen philosophy, but evidently dreads it in
so far as it is susceptible of being turned against religion itself. In
England Montaigne was early popular. It was long supposed that
the autograph of Shakespeare in a copy of Florio's translation
ehowed his study of the Estaya. The autograph has been disputed,
but divers passages, and especially one in The Tempest, show that
at first or second hand the poet was acquainted with tho essayist.
Towards the latter end of the 17th century. Cotton, the frienc. of
Isaac Walton, executed a complete translation, which, though ^.ot
extraordinarily faithful, possesses a good deal of rough vigour. It
has Ijceu frequently reprinted with additions and alterations. Tho
most noteworthy critical handling of the subject in English ia
unquestionably Emerson's in Representative Men. (G. SA.)
MONTALEMBEET, Chaeles Forbes de (1810-1870),
historian, was born on 29th May 1810. The family was
a very ancient one, belonging to Poitou, or rather to^
Angoumois. Direct descent is said to be provable to the
13th century, and charters and other documents carry the
history of the house two centuries fiu-ther back. For some
generations before the historian the family had been dis-
tinguished, not merely in the army, but for scientific attain-
ments. Montalembert's father, Eene, emigrated, fought
under CondS, and subsequently served in the English
army. Hq married a Miss Forbes, and his eldest son
Charles was born at London. At the Restoration Ren6
de Montalembert returned to France, was raised to the
peerage in 1819, and became ambassador to Sv,'eden (where
Claries received much of his education) in 1826. He died
a year after the overthrow of the legitimate monarchy.
Charles de Montalembert was too young to take his seat
as a peer (twenty-five being the necessary age), but he
retained other rights ; and this, combined with his literary
and intellectual activity, made him a person of some
importance. He had eagerly entered iuto the somewhat
undefined plans of Lamennais and Lacordaire for the
establishment of a school of Liberal Catholicism, and he
co-operated with them, both in the Avenir (see Lamen-
nais, vol. xiv. pp. !;39, 240) and in the practical endeavour,
which absorbed some of the best energies of France at the
time, to break through the trammels of the system of state
education. This latter scheme first brought Montalembert
into notice, as he was formally charged with unlicensed
teaching. He claimed the right of trial by his peers, and
made a notable defence, of course with a deliberate intention
of protest. His next most remarkable act was his participa-
tion in the famous pilgrimage to Rome of his two friends.
This step, as is well known, proved useless to mitigate the
measures which private intrigues, and perhaps a not alto-
gether injudicious instinct, prompted the Roman curia to
take against the Avenir and the doctrines of its promoters.
Montalembert, however, submitted dutifully to the ency-
clical of June 1835, and only devoted himself more
assiduously to the work on which he was engaged, the
Life of St Elisabeth of Hungary. This appeared in 1836.
It displayed Montalembert's constant literarycharacteristics,
and, though inferior to Les Moines ^Occident in research
and labour, is perhaps superior to it as a. work of art.
The famous speech by which Montalembert is best known,
— " Nous sommes les fils des croisSs et jamais nous ne re-
culerons devant les fils de Voltaire ", expresses, or at least
indicates, his attitude not insufficiently. He was an ardent
student of the Middle Ages, but his mediaeval enthusiasm
was strongly tinctured with religious sentiment, and at tho
same time by no means connected with any afi'ection for
despotism. Montalembert still climg to his early liberalism,
and he made himself conspicuous dtu-ing the reign of Louis
Philippe by his protests against the restrictions imposed
on the liberty of the press, besides struggling for freedom
in national education. The party which he represented,
or rather which he strove to found, was by no means wholly
Legitimist at heart, and at the downfall of Louis Philippe
Montalembert had .no difficulty in accepting the republic
and taking, when elected, a seat in the assembly. He
had not a little to do with the support given by France to
the pope. As he had accepted the republic, he was not
disinclined to accept the empire ; but the measures which
772
M O N — M O N
followed the coup d!Hat disgusted him, though he still sat
in the chamber. A defeat in 1857 put an end to his
parliamentary appearances. He was still, however, recog-
nized as one of the most formidable of the moderate
opponents of the empire, and he was repeatedly prosecuted
for anti-imperialist letters and pamphlets. In the ten
lyears between 1840 and 1850 he had written little but
political pamphlets, but after the establishment of the
empire, and especially after ho lost his seat in the chamber,
•he became more prominent as an author. Even before
ithis he had produced a volume on the A venir Politique de
TAnc/leterre (\855), and another on Fie IJC. et Lord Palmer-
tton (1856), besides numerous articles and pamphlets, the
,chief of which were perhaps Une Nation [Poland] en Dcuil,
and L'jSglise Libre dans l'£tat Libre.
J His great work, the fruit of many years' labour, did not
appear tiU he was fifty years old, and ten years before liis
death, which occurred before its completion. Les Moines
dOcddent depuis St Benott jnsqu'd, St Bernard has some
of the peculiar drawbacks which have characterized ahnost
all historical work of any literary pretensions during the
present generation. It is planned on too large a scale,
and executed with too- much record to profusion of pictur-
esque detail and abundance of fluent argument on points
which the writer has at heart. Its best passages are inferior
to the best of a younger writer of very different opinions
though not dissimilar style and temperament — M. Ernest
Renan ; but it is a work of great interest and value.
Montalembert, who had mamed Mademoiselle de Merode,
sister of one of Pius IX. 's minister-s, but who had no male
offspring, died in March 1870, the year so fatal to France.
His health had long been very bad, and was understood
to have suffered from the chagrins attending his exclusion
from political life and the defeat of most of his plans.
Since his death his works have appeared in a complete
edition. They have, regarded from the literary point of
Tiew, many of the faults of their time. A voluminous and
vigorous writer, Montalembert was more of a journalist, a
pamphleteer, and an orator than of a man of letters properly
80 called. His talents were diffused rather than concen-
trated, and they were much occupied on merely ephemeral
topics. But of picturesque eloquence in a fluent and rather
facile kind he was no inconsiderable representative.
MONTALVAN, Juan Pekez de (1602-1638), Spanish
dramatist and writer of fiction, was the son of the kiug's
bookseller, and was born at Madrid iu 1602. At the early
age of seventeen ho became a licentiate in theology, and in
1626, after entering the priesthood, he received a notarial
appointment in connexion with the Inquisition. His
overtasked brain succumbed under the numerous Literary
labours he imposed on it, and he died when only thirty-
six years old ("25th June 1638).
In 1624 ho published eight prose tales {Succsos y prodigios en
am-or, en ocho novelns cjcmplarcs), one of which, " The Disastrous
Friendship," has been characterized by Tickoor as one of the best
in the language. This, as well as a subsequent volume of stories
(Para todos:^ Exemplos morales, humams y divines, 1633), was fre-
quently reprinted. His last prose writing was a popular panegyric
on his lately deceased friend and master Lope de Vega {Fama pds-
ttcma de Lope de Vega, 1638), whom he almost rivalled in dramatic
productivencs-s, and whose conventional manner, ilimsiiiess in (-on-
struction, and carelessness iu execution he too closely followed.
The first volume of his collected Comedias appeared in 1638, the
second in 1639. On the Spanish stage they were in great request,
and Montalvan'a repute led inferior WTitors in some cases to borrow
his name. His dramas are distinctly superior to his " Auf os sacra-
montales," but even of the former the tra,r;ody Los Anvintcs de
Tentel is the only one that has enjoyed permanent popularity.
SeeTicknor, Hist: of Span. Lit., vol. ii. (1863).
MONTANA, one of the north-western Territories of
the United States, is limited on the N. by British Columbia,
on the E. by Dakota, on the S. by Wyoming and Idaho,
and on the W. by Idaho. Its boundaries, as established
by statute, are as follows : — on the N., the 49th parallel •,'
on the E., the 27th meridian west of Washington, or the
104th west of Greenwich; on the S. and W. the boun-
dary follows the 45th parallel from the 27th meridi.an weEt
to the 34th meridian west, then turns south along the
latter meridian to its point cf intersection with the conti-
nental watershed, thence aloEg the crest-line of this water-
shed "westward and north-westward until it reaches the
Bitter-root Momitains ; it then follows the crest of this
range north-westward to the fioint where it is crossed by
the 39th meridian west, which it follows uorih to the line 'of
British Columbia. The total 3rea is about 146,080 square
miles — an approximate estimate, as the boundajy along the
continental watershed and the Bitter-root Mountains has
not been exactly surveyed. The average elevation above
sea-level has been estimated at 3900 feet.
Topogi-aphically, Montana may be separated into two
great divisions — that of the ;plains comprising the eastern
two-thirds, and that of the mountains comprising the
western portion. The former, a monotonous roUing ex-
pans?, broken only by the beds of the few streams which
traverse it, and by a few small groups of hills, extends over
niio degrees of longitude in a gentle uniform slope, rising
from 2000 feet above the sea at the eastern boundary to
4000 at the base of the Rocky Mountains. Except along the
streams and upon the scattered groups of hilh), this section
is entirely devoid of foresti-growth of any kind. Vegetation
is limited to the bimch grasses, artemisia, and cacti The
grasses are the mo.st abundant and luxm'iant near the
mountains, where the rainfall is greatest. The mountain
section, comprising the western third of the Territory, is
composed, in general terms, of a succession of ranges and
valleys rumiing very uniformly somewhat in a north-west
and south-east direction. The mountains vary in height
from 8000 to 10,000, even in isolated cases reaching
11,000 feet, with mountain-passes 6000 to 8000 feet above
the sea. Towards the north the ranges become almost
continuous, forcing the streams into long iov\ circuitous
courses in order to disentangle themselves from the maze
of mountains, while, on the other hand, the n.iiges of the
south-v.-estcn part of the Territory are much liroken, afford-
ing nuraerons low passe? and water-gaps.
In the mountainous p.irt of the Territory are the head-
waters of the Missouri (Atlantic basin) and Clark's Fork of
the Colmnbio. (P.i.cific basin). The former rises in the
south-w2st of tho territory in three large branches, the
Jefferson, Madison, and Gallatin, which meet at the foot
of the Gallatin valley at a point kiicm as the " Three
Forks of the Missouri." Here the Jlissouri is a good-sized
stream, fordable with difficulty even when the current is
lowest. From this point to its mouth navigation is pos-
sible when the stream is not below its mean height; it
is interrupted only at the Great Falls of the ilissoiu-i, near
Fort Benton, abovo which, however, it is practically little
used for navigation. Its other principal tributaries iu its
upper course are the Sun, Teton, Marias, Musselshell, and
Milk rivers, all of which vary much in size vrith the season,
—the last two being nearly or quite dry near their mouths
in the fall cf the year. Tho Yellowstone, one of the most
important ti-ibutaries of the Missouri, has nearly all its
course in Jlontana, and is navigable for small steamers as
far as the Cr'ow Agency, except when the water is low.
Clark's Fork of the Columbia is formed by the junction of
the Flathead and the Missoula or HcUgate river. Tho
former rises in the mountains of British Cohuubia and
flows nearly south through Flathead Lake to its point of
junction with the illissoula. The latter rises opposite the
Jeficrson river and flows north-westward, receiving on it«
way several large affluents. Below the point of jimction
of these streams, Clark's Fork flows north-west along tho
MONTANA
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MONTANA
773-
base of the Bitter-root Mountains into Idaho. This stream
is very rapid, and is not narigable. Its course, as well as
those of most of its tributaries, passes through narrow
valleys, the surrounding country being well watered end
covered with dense forests of Conifers.
Otology. — Most of tie mountain area belongs to the Eozoic and
saurian formations. Along the base of the mountains is a Triassic
belt of variable width. Succeeding this is a broad area of nearly
horizontal Cretaceous beds, followed by the Tertiary formation,.
which covers nearly one-third of the Territory. These recent for-
mations are interrupted here and there by volcanic upheavals.
Climate. — The climate of Montana diifers almost as greatly in
different parts of the Territory as that of California. In the north-
west it resembles that of the Pacific coast The westerly winds
hlovring off the Pacific do not meet with as formidable a barrier aa
iarth-.r south, and consequently are not chUied, or deprived of so
large a proportion of their moisture. The result is that the north-
western portion of Montana enjoys a mild temperature and a rainfall
Bufficieut for the needs of agriculture. The valleys of the Kootenai,
Flathead, Missoula, and Bitter-root can be cultivated without irriga-
tion with little danger of loss from drought Farther east and soafii
the rainfall decreases. In the valleys of the upper Missouri, tho
Jefferson, Madison, Gallatin, and tho upper Yellowstono irrigatioa
is almost everywhere required, as well, as over the broad extent of
the plains. Over most of the Territory the rainfall ran^s from 30
to 15 inches annually ; in the north-western comer it rises to £5.
The general temperature is comparatively mild for tho latitude,
the elevation above the sea being decidedly less than that of tho
average of the Rocky Mountain region. The mean annual temper-
ature ranges from 40° to 60" Fahr. , but the variations aro very great
and violent Frosts and snowstorms are possible during every
month of the year, so that agricultiu-e and stock-raising are more
or less hazaraous. On the other hand, the ordinary eitremes ot
temperature are not so great as in more arid portions of the country.
Forests. — Throughout the Territory, as everywhere else in tho
Cordilleran region, forests follow rainfall. The plains are treeless ;
the mountain valleys about the heads of the Missouri are clothed
only with grass and artemisia, many localities extending to a con-
siderable height up the mountains, which are themselves timbered,
though not heavily. In the north-western part, roughly defined
as the drainage area of Clark's Fork, where the rainfall is somewhat
greater, the forests become of importance. The mountains are forest-
Sketch Map of Montana Territory.
dad from summit to base ; and the narrower valleys are also covered,
while the timber is of larger size and of much greater commercial
value than elsewhere in the Territory,— the valuable timber consisting
entirely of the various species of Cont/crK, pine, fir, cedar, &c. Of the
broad-leaved species, willow, aspen, and cotton-wood are abundant.
Fauna.— The native fauna is not sharply distinguished from
that of neighbouring States and Temtories. The higher latitude
is, however, indicated by the relatively greater abundance of species
favouring a colder climate. The moose and the Rocky Mountain
goat, though by no means abundant, still frequent chosen haunts
ui the mountains, — the former in the cool marshy valleys, the latter
npon the most rugged inaccessible elevations. The ijlack-tailed
and mule deer, the antelope, elk, and mountain sheep ar? abundant,
and the bison still ranges the plains, though in sidly reduced
numbers. Among Carnivorte, the bhck and grizzly bjars, mountain
lion, lynx, wild cat, and several species of wolves are stiU plentiful.
' Agrieulture and Industry. — Agriculture is depeadent in most
parts, of Montana upon tho supply of water furnished by the
streams. 0»-ing to this fact it is probable that not more than
8 per cent of the totol area of the Territory can ever, even under
the most economical distribution of the water-supply, be brought
uder cnltivatiOD. In the drainage area of Clark's Fork are
several fine valleys containing 3 considerable extent of arabl;
land, such as those of the Missoula, Bitter-root, Deer Lodge, Jocko,
and Flathead. Upon the head-waters of the Missouri is also & ;.-.r;c
extent of arable land. The valleys of the Jefferson and Madison .^Uo
deserve mention. Along the eastern base of the mountains, near
the head-waters of the Sun, Teton, and Marias rivers, are consider-
able areas susceptible of irricration. Below the Forks the Missoii.-i
flows for 75 miles through a broad vall'ey, much of which can be irri-
gated ; below Fort Benton, however, the blufls become higher and
close in on the river. The Yellowstone, also, after lea-i-ing the monu-
tains, flows through a similar kind of valley, which extends rrith a
few minor breaks down to the point where the river turns from an ecvt
to a north-east course, when it enters a country of mauvaists terns,
which, except as a mausoleum of fossil remains, is utterly valueless.
Owing to the comparatively isolated position of the Territory,
agricultural pursuits have been limited by tho demands of home
consumption. The census of 1880 reported the area in farms to crin-
sist of 405,683 acres, with an avcr.ige of 267 acres to each farm. The
whole Is less than one-half per cent of the entire area of the Ter.-=-
tory. The improved land is reported as amounting to 262,^v,
acres. The following are the amounts of tho principal agricultural
products :— wheat 469,688 bushels: maize, 5689 buphels ; oais^
774
M O N — M 0 N
900,915 bushels ; barley, 30,970 bushels ; hay, 63,947 tons ; wool,
99j'484 pounds ; — value of all fann products, 82,024,923. The live-
stock interest is large, and is increasing rapidly. The great extent
of pasture afforded by the plains ana the broad valleys of the
mountains would seem to promise an almost unlimited e.^ttension
of this industry in the future. Both cattle and sheep owners,
however, labour under disadvantages as compared with the owners
farther south. The lower temperature and heavier snows, and
particularly the danger of great e.^tTemes of temperature, require
that provision of shelter and food be made for a part or all of the
winter season, otherwise the rancheman runs the risk of occasional
severe losses. The census of 1880 furnishes the following statistics
of live-stock : — horses, 35,114 ; mules and asses, 858 ; workingoxen,
93G; milch cows, 11,308; other cattle, 160,143; sheep, 184,277;
swine, 10,278 ;— total value of live-stock, 85,161,554.
In mineral production Montana has never taken a leading place,
although in the early days some of the placer ground yielded well.
Tlie rich placers of Little Prickly Pear, Bannack, and Alder Gulch
were quickly exhausted. The produce of the latter has been reported
variously at from §25,000,000 to ?40,000,000, the greater part of
which was extracted in a few months. In the year 1879-80
$1,805,767 worth of gold and §2,905,068 of silver were cxtractcj,
about three-fourths from deep mines and one-fourth from placers.
For the year 1882 the total mineral production is reported at
$8,004,000, of which about §1,000,000 was for copper and lead.
Population. — Owing largely to its remote position the population
as well as the material prosperity of Montana have had a slow growth
in comparison with other more favoured poi-tions of the west. The
population in 1880, as reported by the census, was 39,159 (28,177
males, and 10,982 females), — an increase of 90'1 per cent, over that in
1870. There were 27,6SS natives, and 11,521 of foreign birth, while
35,385 were whites, 34 6 negioes or of mixed negro blood, 1765 Chinese,
and 1663 citizen Indians. By far the greater portion of the popula-
tion is found in the western half, upon the head-waters of the Missouri
and Clark's Fork. The eastern half is ;is yet but very sparsely settled,
and probably it will never sustain more than a small population.
The Territory is divided into eleven counties, which,' with their
population in 1880, were the following: — Beaverhead, 2712;
Choteau, 305S ; Custer, 2510 ; Dawson, 180 ; Deer Lodge, 8876 ;
Gallatin, 3643 ; Jefferson, 2464 ; Lewis and Clark, 6521 ; Madison,
3915 ; Meagher, 2743 ; Missoula, 2537. The principal settlements
are— Helena, the capital (3624) ; Butte, a mining town (3363) ;
and Bo2eman, in the Gallatin valley upon the Northern Pacific
Kailway, which in 1880 had a population of 894 and has probably
double that number at present (1883).
The total number of Indians in Montana ia estimated by the
Indian office at 19,764. These are nominally congregated at five
agencies, although in reality they roam over the entire Territory.
They are of various tribes, the principal of which are the Sioux,
Crow, Blackfoot, Gros Ventre, Assinaboine, and Pend' d'Oreille.
Their reseivations cover more than one-third of the Territory.
Gomrnment and Fviance. — The government of Montana is similar
to that of the other Territories. Tho governor, secretary, chief jus-
tice, and two associate justices are appointed by the president of tho
United States. The treasurer, auditor, and superintendent of public
instruction are elected by the people of tho Territory, as are also tho
members of the two houses of tho legislature. Montana is repre-
sented in Congress by a delegate, also elective, who has liberty to
take part in debate but has no vote. The Territorial debt at tho
close of 1881 was but §70,000. The amount raised by Territorial
taxation was §93,211.
History. — The Montana country was originally acquii'ed by the
United States under the Louisiana purchase. It became successively
a part of Louisiana Territory, of Missouri Territory, of Nebraska
Territory, and of Dakota. On 26th May 1864 it was organized
under a Territorial government of its own, with practically its present
boundaries. Tho exploration of this region commenced with the
celebrated expedition of Lewis and Clark in 1803-1806. Between
1850 and 1855 it was ti-aversed and mapped by a number of exploring
parties, having in \-iew tho selection of trans-continental railroad
routes. Since then numberless expeditions have examined it, and
somo systematic topographic work has been done under difl'erc^nt
branches of the United States Government. The first settlers
entered the Territory in 1861, discovered placer gold on Little
Prickly Pear Creek, and shortly after built the city of Helena.
Later, the placers at Bannack were discovered, and a small " rush "
to the Territory commenced. In 1863 tho rich placei-s at Alder
Gulch were brought to view, and miners and adventurers swarmed
in from all parts. Then it was that the early social history of Cali-
fornia was repeated on a smaller scale in Montana. Tlio lawless
dements assumed control, and for many months neither life nor
property was safe. Indeed, for a timo tho community was in a
state of blockade ; no one with money in his possession could get
out of tho Territory. Finally, tho citizens organized a " Vigilance
Committee " for self-preservation, took tho offensive, and after a
short sharp struggle rid the cuinmunity of its disturbing clemv^nts.
After tho exhaustion of tho placer?, tho population decreased, owing
to the migration of the floating mining class ; but their place wa.s soon
taken by more permanent settlers. (H. G*.)
MONTANISM is a somewhat misleading name for the
movement in the 2d century which, along v/ith Gnos-
ticism, occupied the most critical period in the history of
the early church. It was the overthrow of Gnosticism and
Montanism that made the " Catholic " church. The credit
of first discerning the true significauca of the Montanistic
movement belongs to Eitschl.^
In this article an account will be given of the general
significance of Montanism in relation to the history of the
church in the 2d century, followed by a sketch of its origin,
development, and decline.
1. From the middle of the 2d century a change began
to take place in the outward circumstances of Christianity.
The Christian faith had hitherto been maintained in
a few small congregations scattered over the Roman em-
pire. These congregations were provided with only the
most indispensable constitutional forms, neither stricter
nor more numerous than were required bj' a religious
bond resting on supernatural expectations, strict discipline,
and brotherly love {" Corpus sumus de conscientia re-
ligionis, de unitate disciplinos, de spei foedere"). This
state of things passed away. The churches soon found
numbers within their pale who stood in need of super-
vision, instruction, and regular control. The enthusiasm
for a life of holiness and separation from the world,
the eager outlook for the end of the world, the glad
surrender to the gospel message, were no longer the
influences by which aU minds were swayed. In many
cases sober convictions or submissive assent supplied the
want of spontaneous enthusiasm. There were many who
did not become, but who tvere, and therefore remained,
Christians, — too powerfully attracted by Christianity to
abandon it, and yet not powerfully enough to Lave
adopted it for themselves. Then, in addition to this,
social distinctions asserted themselves amongst the breth-
ren. Christians were already found in all ranks and
occupations — in the imperial palace, among the officials,
in the abodes of labour and the halls of learning, amongst
slaves and freemen. Were all these to be left in their
callings 1 Should the chui'ch take the decisive step into
the world, consent to its an-angoments, conform to its
cuistoms, acknowledge as far as possible its authorities,
and satisfy its requirements 1 Or ought she, on t!ie other
hand, to remain, as she had been at first, a society of
religious devotees, separated and shut out from tlie world
by a rigorous discipline and working on it only through
a direct propaganda? This was the dilemma that the
church had to face in the second half of the 2d century :
either she must commence a world-\\'ido mission in the
comprehensive sense by an effective entrance into Eoman
society — renouncing, of course, her original peculiarities and
exclusiveness.; or, retaining these peculiarities and clinging
to the old modes of life, she must remain a small insigni-
ficant sect, barely intelligible to one man in a thousand,
and utterly incapable of saving and educating nations.
That this was the question at issue ought to be obvious
enough to us now, although it could not be clearly per-
ceived at the time. It was natural that warning voices
shoiUd then be raised in the church against secular
tendencies, that the well-known counsels about the imita-
tion of Christ shoidd bo held up in their literal strictnes.s
before worldly Christians, that demands should be made for
a restoration of the old discipline and severity, and for a
return to apostolic simplicity and purity. The church as a
whole, however, under pressure of circumstances rather than
by a spontaneous impulse, decided otherwise. She marched
through the open door into the Eoman state, and settled
' En'jtfhting der AWMthoUschcn Kirchc, 2d td., Boan, 1857.
MONTANISM
775
down there for a long career of activity, to Christiani2e the
state along all its thoroughfares by imparting to it the word
of the gospel, but at the same time leavbg it everything ex-
cept its gods. On the other hand, she funushfed herself with
everything of value that could be takep over from the world
without overstraining the elastic structure of the organiza-
tion which she now adopted. With the aid of its philosophy
she created her new Christian theology; its polity furnished
her with the most exact constitutional forms; its juris-
prudence, its trade and commerce, its art and industry,
were all taken into her service ; and she contrived to borrow
some hints even from its religious worship. Thus we find
the church in the 3d century endowed with all the resources
which the state and its culture had to offer, entering into
r.U the relationships of life, and ready for any compromise
which did not affect the confession of her faith. With
this equipment she undertook, and carried through, a world-
mission on a grand scale. But what of those believers of
the old school who protested in the name of the gospel
against this secular church, and who wished to gather
together a people prepared for their God regardless alike
of niunbera and circumstaiices 1 Why, they joined an
enthusiastic movement which had originated amongst a
small circle in a remote province, and had at first a merely
local importance. There, in Phrygia, the cry for a strict
Christian life was reinforced by the belief in a new and
final outpouring of the Spirit, — a coincidence which has
.been observed elsewhere in church history, as, for instance,
in the Irvingite movement. The wish was, as usual, father
to the thought; and thus societies of "spiritual" Christians
, were formed, which served, especially in times of persecu-
tion, as rallying-points for all those, far and near, who
sighed for the end of the world and the excessui e ssamlo,
and who wished in these last days to lead a holy life.
These zealots hailed the appearance of the Paraclete in
Phrygia, and surrendered themselves to his guidance. In
so doing, however, thsy had to withdraw from the church,
to be known as " Montanists," or " Kataphrygians," and
thus to assume the character of a sect. Their enthusiasm
and their prophesyings were denounced as demoniacal ;
their exjiectation of a glorious earthly kingdom of Christ
was stigmatized as Jewish, their passion for martyrdom
as vainglorious, and their whole" conduct as hypocritical
Nor did they escape the more serious imputation of heresy
on important articles of faith ; indeed, there was a disposi-
tion to put them on the same level with the Gnostics.
The effect on themselves was what usually follows in such
circumstances. After their separation from the church,
they became narrower and pettier in their conception of
Christianity. The strict rules of conduct which in a former
age had been the genuine issue of high-strung rehgious
emotion were now relied on as its source. Their asceticism
degenerated into legalism, their claim to a monopoly of
pure Christianity made them arrogant. .As for the popular
religion of the larger church, they scorned it as an adulter-
ated, manipulated Christianity. But these views found
very little acceptance in the 3d century, and in the course
of the 4th they died out. Regardless of the scruples of
her most conscientious members, and driving the most
earnest Christians into secession and the conventicle, the
church went on to prosecute her great mission in the
world. And before she was able, as church of the state
and of the empire, to call in the aid of the civil power to
suppress her adversaries the Montanistic conventicles were
almost extinct.
ii. Such is, in brief, the position occupied by Montanism
» in the history of the ancient church. The rise and progress
of the movement were as follows.
At the close of the reign of Antoninus Pius — ^probably
in the j-.;ar ISij (Epiphanius)— Montanus appeared at
.\rdaban iu Phrygia, bringing revelations of the "Spirit"
to. Christendom. It is unnecessary to seek an explanation
of his appearance in the peculiarities of the Phrygian
temperament. The Christian churches had always, held
that prophecy was to be continued till the return of Christ,
although, as a matter of fact, prophets had not Ijen parti-
cul-irly numerous. Montanus claimed to have a prophetic
calling in the very same sense as Agabus, Judas, Silas, the
daughters of Philip, Quadratus, and Ammia, or as Hennas
at Rome. At a later time, when the validity of the Mon-
tanistic prophecy was called in question in the interest of
the church, the adherents of tho new movement appealed
esplicitly to a sort of prophetic succession, in which their
prophets had received the same gift which the daughters
of Philip, for example, had exercised in that very country
of Phrygia. The burden of the new prophecy was a more
exacting standard of moral obligations, especially with
regard to marriage, fasting, and martyrdom. But Mon-
tanus had larger schemes in view. He wished to organize
a -special community of true Christians to wait for the
coming of their Lord. The small Phrygian towns of
Pepu2a and Tymion were selected as the headquarters
— the Jerusaletn, as the prophet called them — of his
church. He spared no effort to accomplish this union of
believers. Funds were raised for the new organization,
and from these the leaders and missionaries, who were to
have nothing to do with worldly life, drew their pay. But
the ecstasy of the prophet did not prove so contagious as
his preaching. Only two women, Prisca and UftT^Tnillfl^
were moved by the Spirit ; like Montanus, they uttersd in
a state of frenzy the commands of the Spirit, which spoke
through them sometimes as God the Father, sometimes as
the Son, and urged men to a strict and holy life. This
does not mean that visions and significant dreams may not
have been of frequent occurrence in Montanistic circles.
But, as chosen and permanent organs of the Paraclete, only
three persons were recognized — Montanus, Prisca, and
Maximilla ; by their side, however, Alcibiades and Theo-
dotus, from a very early date, nlayed an active riart as
missionaries and organizers.
For twenty years this agitation appears to have been
confined to Phrygia and the neighbouring provinces.
How could it be otherwise? To assemble the whole of
Christendom at Pepuza was a rather impracticable pro-
posal But after the year 177 a persecution of Christians,
from some unexplained causes, broke out simultaneously
in many provinces of the empire. Now in these days
every persecution was regarded as the beginning of the
end. It quickened the conscience, and gave more strength
to eschatological hopes ; it. was a call to observe the signs
of the times and the intimations of God's presence. It
would seem that before this time Montanus had disappeared
from the scene ; but Maximilk, and probably also Prisca,
were working with redoubled energy. And now, through-
out the provinces of Asia Minor, in Rome, and even in
Gaul, amidst the raging of persecution, attention was
attracted to this remarkable movement. The desire for a
sharper exercise of discipline, and a more decided renuncia-
tion of the world, combined with a craving for some plain
indication of God's will in these last critical times, had
prepared many minds for an eager acceptance of the
tidings from Phrygii. There the Spirit, whom Christ had
promised to His disciples, had begun His work ; there, at
least, there were holy.Chidstians and joyful mar^rs. The
oracles of the Phrygian prophets became household words
in distant churches, and it was always the more serious-
minded who received them with undisguised sympathy.
And thus, within the large congregations where there was
so much that was open to censure in doctrine and con-
stitution and morals, conventicles were formed in order
776
M^OlN.T a N I s m
that Christians might prepare themselves by strict discipUae
for the day of the Lord.
Meanwhile in Phrygia and its neighbourhood— especially
in Galatia, and also In Thrace — a controversy was raging
between the adherents and the opponents of the new
prophecy. Between 150 and 176 the authority of the
episcopate had been immensely strengthened, and along
with it a settled order had been introduced into the
churches. It need hardly bS said that, as a mle, the
bishops were the most resolute enemies of the Montanistic
enthusiasm. It disturbed the peace and order of the con-
gregations, and threatened their safety. Moreover, it
made demands on individual Christians such as very few
could comply with. But the disputation which Bishops
Zoticus of Cumana and Julian of Apamea arranged with
Maximilla and her following tCrued out most disastrously
for its promoters. The " spirit " of Maximilla gained a
signal victory, a certain Themison in particular having
reduced the bishops to silence. Sotas bishop of Anchialus
attempted to refute Prisca, but with no better success ;
he too had to retire from the field in disgrace. These
proceedings were never forgotten in Asia Minor, and the
report of them spread far and wide. In after times the
only way in which .the disconiiiture of the bishops could
be explained was by asserting that they had been silenced
by fraud or violence. This v,-as the commencement of the
excommunication or secession, whichever it may have
been, of the Montanists in Asia Minor. " I aip piu'sued
like a wolf," exclaimed the spirit that spoke through
Maximillii ; and her admocif-ons about the end became
inore emphatic than.eveir; — "After me there will come
no other prophetess, bur, the end." Not only did an
extreme party arise ia Asia Minor rejecting aU, prophecy
and the Apocalypse of John along with it, but the majority
of the churches and bishops in that district appear
(c. 178) to have broken off all fellowship with the new
prophets, while books were written to show that the very
form of the Montanistic prophecy ■was sufficient proof of
its spuriousness.^
In Gaul and Rome the prospects of Montauism seemed
for a while more favourable. The confessors of the Galilean
Church were of opinion that communion ought to be
maintained vrith the zealots of Asia and Phrj'gia; and
they addressed a letter to this effect to the Roman bishop,
Eleutherus. Whether this is the bishop of whom Ter-
tuUian (Adv. Pra-x., It) relates that he was on the point of.
making peace with the churches of Asia and Phrj'gia —
t.e., the Montanistic communities — is not certain ; it was
either he or his successor Victor. It is certain, at any-
late, that there was a momentary vacillation, even in
Rome. Nor is this to be wondered at. The events in
Phrygia could not appear new and unprecedented to the
Roman Church. If we may believe Tertnllian, it was
Praxeas of Asia Slinor, the relentless •foe of Montanism,
who succeeded in persuading the Roman bishop to with-
hold his letters of conciliation.
Early in the last decade of the 2d century two consider-
able works appeared in Asia Minor against the Kataphry-
gians. The first, by a bishop or presbyter whose name is
not known, is addressed to Abircius bishop of Hierapolis,
and was written in the fourteenth year after the death
of Maximilla, i.e., apparently- about the year 193. The
other was written by a certain ApoUonius forty years
after the appearance of Montanus, consequently about
196. From these treatises we learn that the adherents of
the new prophecy wpre very numerous in Phrygia, Asia,
and Galatia (Ancyra), that they had tried to defend tliem-
* Miltiades, vtpi toO ii.ii Seiv vfioipifrtiv iv inGTaau \a.\flv. '? At
the same time as Miltiades, if not earlier, Apolliaaris of Hierapolis
clio wrote against the MoDtaoitta.
selves in writing from the charges brought against th'>ra.
(by Miltiades), that they possessed a fully -developed
independent organization, that they, could boast of many
martyrs, and that they were still formidable to the church
in Asia Minor. Many of the small congregations had
gone completely over to Montanism, although in large
towns, like Ephesus, the opposite party maintained the
ascendency. Every bond of intercourse was broken, and
in the Catholic churches the worst calumnies wei^J retailed
about the deceased prophets and the leaders of the societies
they had founded.
In many churches outside of Asia Minor a different
state of matters prevailed. Those who accepted the
message of the new prophecy did not at once leave the
Catholic Church in a body. They simply formed small
conventicles within the church ; in many instances, indeed,
their belief in the new prophecy may have remained a
private opinion which did not affect their position as
members of the larger congregation. Such, for example,
appears to have been the case In Carthage (if we may
judge from the Acts of the martyrs Perpetua and Felicitas)
at the commencement of the persecution of Septimiua
S^verus about the year 202. But even here it was
impossible that an open niptiu-e should be indefinitely
postponed. The bishops and their flocks gave offence to
the spiritualists on so many points that at last it could
be endured no longer. The latter wished for more fasting,
the prohibition of second marriages, a frank, courageous
profession of Christianity in daily Life, and entire separa-
tion from the world ; the bishops, on' the other hand,
sought in every way to make it as easy as possible to be a
Christian, lest they should, lose the greater part of their
congregations. The spiritualists would have excluded
from the church every one who had been guilty of mortal
sin ; the bishops were at that time specially anxious to
relax the stringency of- the old disciplinary laws. And
lastly, the bishops were compelled more and more to
take the control of discipline into their own hands; while
the spiritualists, appealing to the old principle that God
alone can remit or retain sins, insisted that God Himself —
i.e., the Spirit — -n'as the sole judge in the congregation,
and that therefore all proceedings must be conducted
according to the directions of the prpphets. On this point
especially a conflict was ine-iitable. It is true that there
was no rivalry between the new organization and the old,
as in Asia and Phrygia, for the AVestem Montanists
recognized in its main features the Catholic organization
as it had been developed in the contest with Gnosticism ;
but the demand that the "organs of the Spirit" should
direct the whole discipline of the congregation contained
implicitly a protest against the actual constitution of the
church. Even before this latent antagonism was made
plain, there yiere many minor matters which were sufficient
to precipitate a rupture in particular congregations. In
Carthage, for example, it would appear that the breach
between the Catholic Church and the Montanistic con-
venticle was caused by a disagreement on the question
whether or not virgins ought to be veiled. For nearly
five years (202-201 ) the Carthaginian Montanists strove
lo remain within the church, which was as dear to them
as it v.-as to their opponents. But at length they quitted
it, and formed a congregation of their o\vn, declaring that
the Catholic Church was henceforth only a body of
" psychic " Christians, because she would not acknowledge
the Spirit whom God had at last jioured out on His people.
It \vas at this junctm-e that TortuUian, the most famous
theologian of the West, left the church of which he had
been the most loyal son and the most powerful «upporter,
and whose cause ho had so manfully upheld against pagans
and heretics. He too had come to the conviction that tie
MO N — M 0 N
777
church at large ■nta given over to worldlinsaa, that she
had forsaken the old paths and entered on a tray that
must lead to destruction. The writings of Tertullian
afford the clearest demonstration that what is called Mon-
taiijaTTi was a reaction against secularism in the church,
and an effort to conserve .the privileges of primitive Chris-
tianity. At the same time, they show no less clearly that
Montanism in Carthage was a very different thing from
the Montanism of Montanus. Western Montanism, at
the beginning of the 3d century, admitted the legitimacy
of almost every point of the Catholic system. It allowed
that the bishops were the successors of the apostles, that
the Catholic rule of faith was a complete aad authoritative
exposition of Christianity, and that the New Testament was
the supreme rule of the Christian life. How, then, 6ne may
well 8^ was it possible to separate from the Catholic
Church 1 On what ground could the separation be justi-
fied 1 How could it be said that a new era of the Spirit
had come in when the Spirit had already given all neces-
sai-y instructions in the Scriptures of the New Testament ?
And what claim could be thought to exceed the legitimate
rights of the successors of the apostles 1 Montanus himself
and his first disciples had been in quite a different position.
In his time there was no fixed, divinely-instituted congrega-
tional organization, no canon of New Testament Scriptures,
"no anti-Gnostic theology, and no Catholic Church. There
were simply certain communities of believers bound to-
gether by a common hope, and by a free organization,
which might be modified to any required extent. When
Montanus proposed to summon all true Christians to Pepiua,
in order to live a holy life and prepare for the day of the
Lord, there was nothing whatever to prevent the execution
of his plan except the inertia and lukewarmness of Chris-
tendom. But this was not the case in the West at the
beginning of the 3d century. At Rome and Carthage,
and in all other places where sincere Montanists were
found, they were confronted by the imposing edifice of tha
Catholic Church, and they had neither the courage nor the
inclination to undermine her sacred foundations. This
explains how the later Montanism never attained a posi-
tion of influence. In accepting, with slight reservations,
the results of the development which the church had
undergone during the fifty years from 160 to 210 it
reduced itself to the level of a sect. For, if the stand-
point of the Catholic Church is once acknowledged, then
Montanism is an innovation ; and if the canon of the New
Testament b accepted the doctrine of a new era of the
Spirit is heresy. Tertullian exhausted the resources of
dialectic in the endeavour to define and vindicate the
relation of the spiritualists to the " psychic " Christians ;
but no one will say he has succeeded in clearing the Mon-
tanistic position of its fundamental inconsistency.
Of the later history of Montanism very little is known.
But it is at least a significant fact that prophecy could
not be resuscitated. Montanus, Prisca, and Maximilla were
always recognized as the inspired authorities. At rare
intervals a vision might perhaps bo vouchsafed to some
Montanistic old woman, or a brother might now and then
have a dream that seemed to be of supematiu^ origin ;
but the overmastering power of religious enthusiasm was a
thing of which the Montanists knew as little as the Catho-
Hcs. Their discipline was attended with egiaUy disap-
pointing resixlts. In place of an intense moral earnestness
binding itself by its own strict laws, we find in Tertullian
a legal casuistry, a finical morality, from which no good
could ever come. It was oaly in the land of its nativity
that Montanism held iJs ground till the 4th century. It
maintained itself there La a number of close communities,
probably in places where no Catholic congregation had
been formed ; and to these the Novatians at a later period
attached themselves. In Carthage there c:\ij»teJ down to
the year 400 a sect called Tertullianists ; and in their
comparatively late survival we have a striking testimony
to the influence of the great Carthaginian teacher. On
doctrinal questions there was no real difference between
the Catholics and the Montanists. The early Montanists
(the prophets themselves) used expressions which seem
to indicate a Monarchian conception of the person of
Christ. After the close of the 2d century we find two
sections amongst the Western Montanists, just as amongst
the Western Catholics, — there were some who adopted tho
Logos-Christology, and others who remained Monarchians.
Sources. — The materials for the history of Montanism, although
plentiful, are fragmentary, and require a good deal of criti^
sifting. They may be divided into four groups. (1) The utterances
of Montanus, Prisca, and Maximilla ' are oar most important sources,
but unfortunately they consist of only twenty-one short sayings.
(2) The works written by Tertullian after he became a Montanist
fiunish the most copious information, — not, however, about the
first stages of the. movement, but only about its later phase, after
the Catholic Church was established. (3) The oldest 4)olemical
works of the 2d century, extracts from which have been preser^'ed,
especiaDy by Eusebius (Hist, Ecdcs.y bk. v.), form the next group.
These must be used with the utmost caution, because even tno
earliest orthodox writers give currency to many misconceptions and
calumnies. (4) The later lists of heretics, and the casual notices
of church fathers from the 3d to the 5th century, though not con-
taining much that is of value, yet contain a little.*
LiUraiure. — Ritschl's investigations, referred to above, super-
sede the older works of Tillemont, "Wemsdorf, Mosheim, Walch,
Neander, Baur, and Schwegler {Der Monianisnius und die christ-
liche Kirche dis 2Un JahrhundertSy TubiDgen,1841). Thelater works,
of which the best and most exhaustive is that of Bonwetsch, Die
QeschichU des ifonianismus, 1881, all follow the lines laid down by
Ritschl. See also, Gottwald, Ve Uiyntanismo TertuHiani, 1862 ;
Riville, "Tertullien et le Montanisme"in ihelU'oue des Deux Mcmdcs,
1st November 1864 ; Stroelin, Essai sur le MorUanisme, 1870 ; De
Soyres, Montanis)n and the Primitive Church, London, 1878 ; W.
Cujiningham, The Churches of Asia, London, 1880; Kenan, ** Les
Crises du Catholicisme Naissant" in Itev. d. Vettx Moiides, 15th Feb-
ruary 1881 ; Moller, art. **Montantsmu3" in Herzog's Theol.
JRealencyklqp., 2d ed. Special points of importance in the history o(
Montanism have been quite recently investigated by Lipsius, Over-
beck, Weizsiicker {Theol. Lit.-Zeitung, Nr. 4, 1882), and Harnack
(Das Mbnchthiim, seine Ideate und seine GeschicfUe, 2d ed. , 1882, and
Z. /. Kircheng., iii pp. 369-408). Weizsacker's short essays are
extremely valuable, and have elucidated several important points
hitherto overlooked. (A. HA.)
MONTARGIS, chief town of an arrondissement in the
department of Loiret, France, lies 40 miles east-north-east
of Orleans on the railway from Paris to Lyons. Travei-sed
by the Loing, Montargis belongs to the basin of the Seine,
but it communicates with the Loire by the Orleans and
the Briare canals. It has a fine church (Ste Magdelaine),
dating in part from the 12th century, a museum, and a
public library ; and it still preserves portions of. its once
magnificent castle, which was capable of containing 6000
men, and, previous to the erection of Fontainebleau, was so
favourite a residence of the royal family that it acquired the
title of " Berceau des Enfans de la France." Paper-making
(introduced in the beginning of the 18th century) and
several other considerable industries are carried on. The
population of both commune and town was 9175 in 1S76.
Montargis {Mons Argi or Algi, M: Arcinus, Monlargium) was
formerly the capital of the Gatinais (Pagus Vastinensis). Having
passed in 1188 from the Conrtenai family to Philip Augustus, it
long formed part of the royal domain. In 1528 Francis I. mortgaged
town, castle, and forest (this last a tract of great value) to Ren^
d'Este, daughter of Louis XIL, the famous Huguenot princess ; and
in 1570 Charles IX. gave them in full property to her daughter Anne,
through whom they descended to the dukes of Guise, but they were
repurchased for the crown in 1612. llontargis was several times
taken or attacked by the English in the 15th century, and is parti-
cularly proud of the successful defence it mede in 1 427. "Both Charles
VII. and Cliarles VIII. held court in the town ; it was the latter who
set the famous 0og of Montargis to fight a duel with his master's
murderer whom he had tracked and captured.
* Collected by Muuter, and by Bonwetsch, OeediicJUe des MonUnr
ismus, p. 197 eq.
* On the souices, see Bonwetsch, pp. 16-55.
XVI. — 98
778
M O JN ~- Ivl O is
MONTAUB.VN, chief town of the department of Tarn-
(!t-Garonne, France, is situated on a slight eminence be-
tween the right bank of tlie Tarn and its tributary streams
the Tescou and Lagarrigue, 12S miles by rail east-south-
east of Bordeau.\. It is connected with the suburb of
Ville-Bourbon on the left bank of the Tarn by a remark-
able brick bridge of the Uth century, which is 672 feet
in length, and consists of seven pointed arches resting on
piers, themselves pierced by jiointed arches. The cathe-
dral, built in 1739, contains the Vow of Louis XIII., one
of the finest paintings of Ingres, a native of Moutauban,
and at the end of the Carmelite walk a monument was
erected to his memory in 1871. In the town-house, once
occupied as a palace by the counts of Toulouse and by
the Black Prince, are the paintings bequeathed by Ingres,
&a archjeological collection, and a very curious library
containing the bequests of several celebrated collectors.
Montauban possesses a Protestant theological college. The
town has some trade in corn, wine, and grapes. The manu-
facture of corn-dressers, coarse cloth, pens, and earthen
and china tvare are the principal industries ; and there
;ire also corn and woollen mills. The population in 1881
was 28,335.
Montauban was only a village in the time of the Romans. In
the 8th century a monastery was founded there by the Benedictines,
v.'ho exercised lordship over the neighbouring population. A
.■onsiderable impetus was in the 12th century given to its prosperity
by a decree of the Counts of Toulouse o.Tering freedom to all serfs
taking up their residence in the town. Montauban was twice
besieged by Simon de Montfort in the Albigensian wars, and was
aacked in 1207. By the treaty of Bretigny (1360) it was ceded
to the EngUsh ; but shortly afterwards they were expelled by the
inhabitants. In 1560 the bishops and magistrates embraced Pro-
Icstantism, expelled the monks, and demolished tho cathedral.
About ten years later it became one of the Huguenot strongholds,
and formed a small independent republic. It was the headquarters
of the Huguenot rebellion of 1 621 , and was vainly besie,ged by Louis
.XIII. for eighty-six days; nor did it submit until after the fall
of Rochello in 1629, when its Ibrtifications were destroyed by
Richelieu. In the same year the plague cut off over 6000 of its
iuhabitants.
MONTBELIARD, chief town of an arrondissement in the
department of Doubs, France, is situated 1020 feet above
the sea at the confluence of the .A.llaine and the Lusine,
tributaries of the Doubs, and on the canal between the
Rhine and the Rhone, about 40 miles north-east of Besangon.
Once a fortified city, it still retains the old castle of the
counts of Montb^liard. A bronze statue^of Cuvier, the
most illustrious native of Montbeliard, and several fine foun-
tains adorn the town, which also possesses a museum of
natural history and antiquities, and a Protestant normal
school. Since 1870 a considerable impetus has been given
to its prosperity by the arrival of Alsatian immigrants.
The industries embrace watchmaking, the manufacture of
graving tools, iron wire, files, watch-springs, and pumps,
cotton spinning and weaving, printing, and tanning. The
chief exports are cheese, leather, and wood. The popu-
lation in 1881 was 8784, of which the great majority were
Protestants.
After belonging to tho Burgundians and Franks, Montb(!liard
was, by the treaty of Verdun (848), added to Lorraine. lu the 11th
century it became the capital of a count.ship, which formed part of
the second kingdom of Burgundy, and latterly of the German
empire. From the end of the 14 th century until 1793 it belonged to
the house of Wiirteinberg. It resisted the attacks of Charles the
Bold, King Louis XII., and the duke of Guise, but was taken in 1676
by Marjhal Luxembourg, who razed its fortifications. In 1871 the
battle of HiSricourt between the French and Germans had its com-
mencement within its walls.
MONT-DORE-LES-BAINS, a village of France in the
department of Puy de Dome, 17 miles as tho crow flies
Bouth-wcst of Clermont Ferrand, 3432 feet above the sea,
on the right bank of tho Dordogno not far from its source.
"ike Monta Dore, from which it takes its name, close the
vaUcy towards the south ; their culminating peak, Puy de
Sancy (6188 feet), is the highest eminence of central France.
The mineral springs of Mont Dore were known lo tho
Romans. Tha eight now used yield 94,600 gallons in
twenty-four hours. Bicarbonate of soda, iron, and arsenic
are the principal ingredients of the water ; to the two last
it owes its efficacy in cases of pulmonary consumption,
bronchitis, asthma, and nervous and rheumatic paralysis.
From the elevation and exposure of the valley, which
opens to the north and runs up towards mountains never
quite free from snow, the climate of Mont-Dore-les-Bain:i
is severe, and the season is consequently short. About
5000 patients visit the place between 15th June and 15th
September, when a casino and theatre are opened. The
chief building is the solid but sombre bath-house (hot
baths). The surrounding country, with its fir woods,
pastures, waterfalls, and mountains, is very attractive. In
the " park " at Mont-Dore-les-Bains, which forms a little
promenade along the Dordogne, relics from the old Roman
baths have been collected, but the ancient estatlishmeut
must have been on a larger scale than the present one. A
pantheon erected about the time of Augustus existed till'
the 16th century. Tlio population in 1881 was 1438.
MONTE CARLO. See Mon.\co.
5I0NTE CASINO (or Cas.sino). The Benedictine
monastery known as the abbey of Monte Cassino is a huge
square building of three stories, built on the usual Benedicts
ine plan (see Abbbv) on the summit of a picturesque isolated
hill, about 3i miles to the north-east of the town of Cassino
(Casinum) or San Germane (population about 5000), which
lies midway between Rome and Naples in the valley of the
Garigliano. The most prominent architectural feature is
the large church (1727), richly decor.ated in the interior with
marbles, mosaics, and paintings. The library and archivio
have been spoken of elsewhere (vol. siv. pp. 531, 548).
The d;ite of Benedict's withdrawal from Subiaco to Cassino is
529. At that time Cassino was the site of a temple of Apollo and
of a grove sacred to Venus. The result of the saint's preaching was
that the natives demolished both, chapels to St Martin and Jola
the Baptist being built in their stead, while farther up the hill a
monastery began to rise. About 589 the monks were driven from
it to Rome by the Lombards of Benevento, and it lay v.aste for
more than a century, until resuscitated by Gregory II. (719). In
787 it received fresh privileges from Charlemagne ; in 884 it was
burnt by the Saracens, and was not restored until about seventy
years later. From 1322 to 1366 the abbot held episcopal rank;
under the houie of Anjon ho bore the title of Alias atbaticm, and
ranked as first baron of the realm. In 1504 the abbey was sacked
by the troops of Gonzalo do. Cordova. In 1866 it shared the fate
of all other religious houses in Italy ; it is now inhabited by a few
monks, and uscil as a seminary, having about 200 pupil's.
MONTECUCULI, Raimondo, Count of (1608-1680),
a prince of the empire and duke of Melfi, a famous Austrian
general, was born at the castle of Montecuculi in Modena,
in 1 608. At the age of nineteen he began his career in a
re;;iment of infantry under his uncle, Ernest, count of
I'ontecuculi ; and during the Thirty Years' War he found
many opportunities of displaying his military genius in- the
imperial service. In 1631, having been severely wounded,
he was made prisoner while retreating after tho battle of
Breitenfeld. Soon after his release he was promotid to the
rank of major ; and he distinguished himself at the siege
of Nordlingeu in 1 634, and at the storming of Kaiscrslautern
in 1635. As colonel, he took part in much hard fighting
in Pomerania and in Bohemia; and in 1639 at Jlelnik,
where he tried to prevent tho Swedes from crossing the
Elbe, he was taken prisoner a second time, being compelled
on this occasion to spend more than two years in Stettin.
The time was not lost, for he devoted it to a thoroui'h study
of military science. In ,1642 he was again at work in tho
imperial army, and for eininent services in Silesia he was
made a major-general of cavalry. After a brief visit to
Italy, during which he entered the service of the duke of
Modena, he returned to Germauy, and became councillor
M O N — M 0 N
779
of Trar in 1644. In tUe iollowing year he supported the
archduke Leopold in a campaign against Prince Rikoczy
of Transylvania, resisted Marshal Turenne in the Rhine
country, and fought with the Swedes in Silesia and Bohemia.
The victory at Triebel in Silesia, in 1647, was due chiefly
to him, and he was rewarded by being raised to the rank
of general of cavalry. After the peace of Westphalia in
1648 he occupied himself for some time with the work of
the council of war ; and in 1654 he undertook diplomatic
jiissions to Christina, queen of Sweden, and to Cromwell.
In 1657 he commanded an expedition against Prince
Hakoczy and the Swedes, who had attacked the king of
Poland, and Rakoczy was soon forced to withdraw from
the Swedish alliance, and to accept terms of peace. As
field-marshal he was sent to the aid of Denmark against
Sweden ; and this war he conducted so successfully that
the peace of Oliva was concluded in 1660. In 1663 he
resigned the command of an army with which, for about
three years, he had been opposing the Turks ; but in 1664
he was again made commander-in-chief, and in the same
year he defeated the Turks so decisively near the abbey of
.St Gotthard that they concluded an armistice for twenty
years. He had to deal with more formidable enemies in
1672, when, the emperor and the imperial diet having
resolved to uphold the Dutch against Loms XIV., Moute-
cnculi, who had been serving as president of the council of
war aad director of artillery, was appointed commander of
the imperial forces. He took Bonn, and, although closely
watched by Turenne, contrived to effect a junction with
the prince of Orange, thereby overthrowing all the calcula-
tions of the French. When the elector of Brandenbiu-g
received the supreme command in 1674 Jlontecuculi with-
drew from the army; but in 1675, being restored to his
former position, he resumed operations against Turenne.
The two commanders manoeuvred so brilliantly that tor
about four months neither could do the other much injury ;
but, Turenne having been killed by a cannon-ball on the 27th
of July 1675, Montecuculi pursued the French into Alsace,
and besieged Hagenau and Zabern, retiring from Alsace only
wheii he found himself confronted by Cond^. MontecucuU's
last achievement in war was the siege of Philippsburg.
During the rest of his life he was president of the council
of war. In 1679 the emperor Leopold made him a prince
of the empire, and shortly afterwards he received from the
lung of Naples the dukedom of Melfi. Having accompanied
the emperor to Linz during the pestilence, he was injured
by the fall of a beam when entering the castle, and died at
linz on the 16th of October 1680.
Montecuculi was an ardent lover of science, and wrote several
important military works. Tlie Opere complete di Monltcuculi were
published in two volumes, at Jlilan in 1807, at Turin in 1821 ; and
there is a German translation (1736) of his Memoris cUlta guerra ed
istntzimii d'un gen^rak.
See Campori, Saimondo Montecuculi, la yja faminHa c t suot tempi (1S77)
MONTELEONE (usuaUy caUed Moutcleono of Cala-
bria to distinguish it from Monteleone of Apulia in the
provhico of Avellino, which gave its name to the medi&jval
duchy of the Pignatelli famUy) is a city of Italy in the
province of Catanzaro, on the western side of the Bruttian
peninsula, and is beautifully situated on an eminence gently
sloping towards the gulf of Sta Eufemia. It was ahnost
totally destroyed by earthquake in 1783, and for many
years afterwards consisted mainly of slight wooden erec-
tions, but under the French occupation it was made the
* capital of a provmce and the headquarters of General
Regnier, and it is now a well-built town. The castle was
built by Roger, count of Sicily, whom tradition accuses of
carrying off the ruins of the ancient temple of Proserpine
to the cathedral of IJileto. The population of the town
was 9244 in 1871, that of the commune 10,262 in 1861
and 12.0!7 : :r-'.
Monteleone is identified with the ancient Hipponium, a Greek
city first mentioned in 389 B.C., when its inhabitants wci-e removed
to Syracuse by Dionysius. Restored by the Carthaginians (io6},
held for a time by Agathoclea of Syracuse (291), and afterwards
occupied by the Bmttians, Hipponium ultimately became as Vibo
Yalentia a flourishing Roman colony. The harboiu: established
by Agathocles proved of great service as a naval station to Casar
and Octavius in their wars with Pompeius Magnus and Sextua
Pompeius, and remains of its massive mason-work still exist at the
village of Bivona on the coast. . In. tha to\ra itself there are no
traces of antiijnity beyond a mosaic pavement in the church of St
Leoluca (patron saint of Monteleone) and one or two Latin inscrio-
tions.
MONTELIMAR, chief town of an arrondissement ana
canton in the department of Dr6me, France, is situat'xl
near the left bank of the Rhone, 93 miles south of Lyons
on the railway to MSirseilles. The waters of the Roubioii
and Jabron, which unite at Montilimar, spread fertility over
the plains surrounding the town. A well-planted park
separates the town from the station, but within the four
gates that still remain the streets are narrow and unin-
viting. The ancient castle, one of the most interesting
military remains of central France, is now used as a
prison. Silk throwing and spinning, and the manufacture
of flowered silks and of hats, are the principal industrie.s ;
there are ako foundries, tool-shops, and tanneries, ami
agricultural implements and hydi-auHc lime are made.
Mont^limar is famed for its nougat, a cake composed of
almonds and honey. The population of the town in 18S1
was 12,894.
Mont«limar was called by the Romans Acusium. At a lattr
period it belonged to the family of Aymar or Adhemar, whence it-,
present name. After coming into the possession of the counts ot
Valentinois, and then of the dauphins of Viennois, it was unitet'
by Louis XL to the crown of France. It frequently changed
hands during the religious wars, and, although it resisted Coliguy,
it was taken iu 1580 by Lesdiguitres.
MONTENEGRO, often pronounced and sometimes
\viitteu JIONTENEEO (Montenegrin, i.e., Servian, Crnagora,
Russian Tcheniogoriya, and Turkish Karadagh, all eq'oi-
valent to Black Mountain), one of the smallest of Euro-
pean countries, lies on the eastern side of the Adriatic,
and is bounded by Dalmatia, Herzegovina, Bosnia, end
Albania. Previous to 1878 it had an area variously esti-
mated at 1Q69 square miles (Kaptsevitch), 1711 (Kiepert),
and, including the Kutclii territory, 1796 (Bebm). The
enlatgement to about 5272 square miles proposed by the San
Stefano treaty (1878) would probably have swamped the
Montenegrin nationality, and the Berlin congress brought
the total area only up to 3680 miles, or almost exactly half
the size of Wales, i
Apart from her new maritime district, Montenegro seems
^ Since 1870 several rectifications of frontier and exchanges of
territory have been arranged between Montenegro and Turkey, but
these h.-'.ve left the area practically undisturbed. All the figures are
approximate estimates, as the only geodetic survey of the country,
carried out by Russian officers, is still (1883) in progress. The old
frontier line had the great disadvantage to the Montenegrins of leaving:
the fortress of Niksitch in the nortb-weat, and that of Spuzh in the
south-east in the hands of the Turks, who thus commanded the valley
of the Zeta, and sti'ategically almost cut the country in two, the distance
from the frontier near Niksitch to the frontier near Spuzh being only
some 15 miles. The present frontier includes not only these strong-
holds, but also those of Podgoritza, Zhabliak (Jablac), and Lesendr.^
a great part of Lake Scutari, and the coast district with Antivari
and Dulcigno. To get access to the sea had long been the ambitiou
of Montenegro, which in her early days had possessed not only
Dulcigno but Durazzo, and had surrendered them to purchase from
Venice assistance in her struggle against the Turks. The Berlin con-
gress gave her the coast from Cape Maria to Cape Kruci or Krutcb,
but Spizza, the harbour to the north, was retained by Austria, and
Dulcigno, to the south, by Turkey. In the beginning of 1880, by tho
Corti compromise, the Kutcbi territory and the plain ot Podgoritza
were accepted by Montenegi*o in lieu of Plava and Gussinye, assigned to
her by the congress ; but the exchange was deferred, and the terma
ultimately mcditied by the congress so as to include Dulcigno in
Montenegrin territory. The occupation of the district (November
1880) was only eSected after a naval demont'lration ou the psriof tho'
i^Tcat powers.
780
MONTENEGRO
little better .at first than a chaos of mountains, but on
closer- examination it appears that there are two distinct
groups, an eastern and a western, divided by the Zeta-
Moratcha valley. The loftiest summit is Dormitor, 8146
feet high, in the new territory near the north frontier,
next come Kom Kutchi (8031), Kom Vassoyevitzki (7946),
and Dormitor Schlime (7936).' Had the original frontier
of the Berlin congress towards the south-east been retained
it would have run along the still higher Prokletia range.
Many of the mountain-tops remain white ■with snow for
the greater part of the year, and from some of the dark
ravines the snow never disappears. The south-western
portion of the country consists of limestone, the north-
eastern mainly of Paleozoic sandstones and schists with
underlying trap.'' In their general aspect the two regions
ara strikingly distinct. The former seems, as it were, one
enormous mass of hard crystalline rock, bare and calcined,
with its strata dipping to the south-west at an angle often
of 70 degrees. Its whole surface has been split by atmo-
sjiherio agencies into huge prismatic blocks, and the cracks
Map^ of Montenegro,
have been gradually worn into fissures several fathoms deep.
In some places the process has resulted in clusters of im-
mense sharp-pointed crags, the sides of which are furrowed
by rain-channels, while in others there are countless funnels
running down into the rock for 200 feet and more. In
like manner the interior of the mass is hollowed out into
immense galleries and caves, and during the rainy season
subterranean landslips frequently produce local earthquakes,
extending over an area of 10 or 12 miles. The sandstone
region, on the other hand, presents lofty but rounded
forms, clothed for the most part with virgin forest or rich
alpine pasture, broken here and there by dolomitic peaks.
' Bull, de la Soc. de Qiogr., Paris, 1881.
^ Dr Tietze, whose full report w.na to appear in the Jahrb. der Reichsan-
atalt for 1883, informed the writer that the existence of the following
formations in Montenegro h.is been clearly ascertained : — (1) Palaeozoic
•chlsts, (2) Wirfen strata of Lower Trias, (3) Trap of the Pala-ozoic
and Wirfen strata, (4) Triaasic limestone, (5) Jurassic limestone, (6)
Cretaceous limostouo, (7) Klysch, in part certainly Eocene, and (8)
Keogcnic or younger Tertiary fomiutions. The existence of nuromulitic
limeatoue is ctill doubtful.
The watershed tetween the Adriatic and the Black Sea
crosses the country from west to east in a very irregular
line, the southern districts being drained by the Zetar
Morateha river sy.stem, which finds its way to the Adriatic
by Lake Scutari and the Boyanna, while the streams of
the northern districts form the head-waters of the Drina,
which reaches the Danube by way of the Save. The Zeta,
rising in Lake Slano, is remarkable for its subterranean
passage beneath a mountain range 1000 feet high. At a
place called Ponor the water plunges into a deep chasm,
seeming almost to lose itself in foam, but at a distance of
several miles it reappears on the other side of the mountains.
Its whole course to its junction with the Jloratcha is
about 30 miles. Rising in the Yavorye Planina, the
Morateha sweeps throiigh the mountain gorges as a foam-
ing torrent till it reaches the plain of Podgoritza ; then,
for a space, it almost disappears among the pebbles and
other alluvial deposits, nor does it again show a current of
any considerable volume till it approaches Lake Scutari.
In the neighbourhood of Duklea ^ and Leskopolye it flows
through a precipitous ravine from 50 to 100 feet high.
In the dry season it is navigable to Zhabliak. The whole
course is about 60 miles. Of the left-hand tributaries of
the Morateha the Sem or Tsievna deserves to be mentioned
for the magnificent canon through which it flows between
Most Tamarui and Dinosha. On the one side rise the
mountains of the Kutchi territoiy, on the other the
immense flanks of the Prokletia range, — the walls of the
gorge varying from 2000 to 4000 feet of vertical height.
Lower down the stream the rocky banks approach so
close that it is possible to leap across without trouble.
The Eyeka issues full-formed from an immense cave south-
east of Cettinye (Tsettinye) and falls into Lake ScutarL
The three tributaries of the Drina which belong in part to
Montenegro are the Piva, the Tara, and the Lim, respect-
ively 55, 95, and 140 miles in length. The Tara forma
the northern boundary of the principality for more than 50
miles, but the Lim leaves the country altogether after the
first 30 miles of its course. Great alterations have taken
place on Lake Scutari in recent times. The river Drin,
which previous to 1830 entered the Adriatic to the south
of Alesia near S. Giovanni di Medua, subsequently changed
its course so as to join the Boyanna just below its exit from
the lake ; one of the chief results has been to raise the
level of the lake, and so to flood the lower valleys of the
tributary streams. When the International Frontier Com-
mission was at Scutari in April 1879, the water stood 8 feet
deep in some of the principal streets, and the inundation
of city and suburbs lasted that year eight n;onths. A few
small lakes are scattered among the mountains, and it is
evident that their number was formerly much greater. The
plain or hollow of Cettinye was doubtless filled with water
at no very distant (geological) date, and even now, when
the sudden rains cannot escape fast enough by the ordinary
subterranean outlet, the royal village sufi'ers from a flood.
If the new territory be left out of view, there is but
little farming land in Montenegro ; the peasant is glad to
enclose and protect the veriest patches of fertile soil retained
by the hollows in the mountain sides, and one may sea
" flourishing little crops not a yard square." " The largest
landed proprietor is the holder of 60 acres" (Denton,
Montene<jro, p. 143) ; the other freehold estates vary from
2 to 20 acres, and it is usually not to the individual but
to the house or family that the ownership belongs. Woods
and pastures ai-o the common property of the clan (pleme).
The people live in small stone-built cottages, grouped for
the most part in little villages, and their whole life is
' Duklea Is the name still borne by tlie ruins of the Roman Docloa,
ftou, but wrongly, called Dioclea from its association with the family
I of Dioelctian. --"
M O N — M O N
781
marked by extreme tdmplicity. Chastity is a national
virtue, and in time of war the women and children of the
Turks have often found their safest asylum among their
hereditary foes. The main stock of the people is of Servian
descent ; and, though the purity of both blood and language
has been to some extent affected by foreign elements, mostly
Albanian and Turkish, the national imity has not been im-
paired. The curious Gipsy colony, which, though speaking
Servian, never intennaiTies with the Montenegrins, is
numerically of little importance.' The great mass of the
people belong to the Orthodox Greek Church, only some
7000 being Eoman Catholics, and 3000 Mohammedans.
According to Kaptsevitch, the population was 10,T00 in
1838, 120,000 in 1849, 124,000 in 1852, and 170,000 in
1877, but in 1879 it was found that, inclusive of the new
territory, the number could not exceed 150,000; since then
abeut 15,000 have been added with Dulcigno. The official
returns for 1882 (not based on a census, however) give
236,000 as the total, of whom some 23,000 live in the
so-called towns.
Fauna. — Bears are still found in the higher forests, and wolves,
and especially foxes, over a much wider area. A. few cliamoia loam
on t!»e loftiest summits, the roebuck is not infrequent in the
backwoods, the wild boar may be met with in the same district, and
the hare is abundant wherever the ground is covered with herbage.
There aro one or .two species of snakes in the country, including the
poisonous lUyriaa viper. Esculent frogs, tree frogs, the common
tortoise, . and vai-ious kinds of lizards are all common. The list of
bii'ds observed by Baron Kaidbara includes golden eagles and vul-
tures, 12 species of falcons, several species of owls, nightingales, larks,
buntings, lioopoes, partridges, herons, pelicans, ducks (10 species),
goatsuckers, ic. The abundance of fish in Lake Scutari and the
lower course of the Ryeka is extraordinary, the shoals of bleak (scor-
antza, Leuciscxis albumua) that come up the river forming almost
solid masses. Both trout and salmon aro caught in the Moratoha.
Flora. — The flora of Montene^-o is comparatively scanty. In
the forest districts the beech is the prevailing tree up to a height
of 5000 or 5500 feet, and then its place is taken by the pine. The
chestnut forms little groves in the country between the sea and
Like Scutari, but never ascends mo-e than 1000 feet, and the
olive also is mainly confined to the neighboui-hood of the Adriatic.
Pomegranate* bushes grow wild, and in many parts of the south
cover the foot of the hills with dense thickets, the rich blossoms of
which are one of the special chai-ms of the spring landscape. Wheat,
rye, barley, maize, capsicums, and a little tobacco are grown in the
north, and in the south, vines, figs, peaches, apples, cherries, citrons,
oranges, &c The potato, introduced in 1786, is cultivated con-
siderably beyond the local demand ; the planting of mulberry trees
and the rearing of silk-worms is of growing economical importance.
roicM.— Ckttinyk (g.i!.), with about 2000 inhabitants, is the
capital of the country. Podgoritza (about 6000 or 7000 in 1879,
since reduced to 4000) is the principal trading town ; it lies at the
foot of the mountains (as its name imports), at the junction of the
Ruibnitza with the Moratcha, and in Turkish hands was one of the
strongest of their fortresses towards Montenegro. Dulcigno (see
vol. vii. p. 520) has 3000 inhabitants (before the transfer 5000 to
7000). Niksitch, a fortified place on a slight eminence in the
midst of a plain, is about the same size. Antivari (see vol. ii. p.
138), so called from its position opposite Bari in Italy, suffered
greatly in the war 1879-80, and lost half of its 6000 inhabitants.
panilovgrad, with 2000, lies on the north side of the Zeta valley ;
in the vicinity is Orialuka, the prince's palace with its mulberrj-
nurseries, and the monasteries of Zhdiebanik (burnt by the Tmks in
1877, but since rebuilt), while Tcheliya, Moratcha (the most aucicnt
in the principality), and Ostrog (visited annually by about 10,000
l.ilgrims) are not far off. Spuzh (Sponge), a little lower on the
.same side of the stream, is a fortified post with about 1000 inhabit-
onts. Nyegush or Nyegosh (1200), about three hours distant fiom
Cettinye on the road to Cattaro, is the native seat of the reigning
family, which originally came thither from Nyegush in Herzegovina.
Zhabliak (^1200) was rnce the "capital," and has been a fortified
post since the time of the Venetian power Ryeka (1600), on the
river of that name, is next to Podgoritza in commercial importance ;
the prince has two residences in the town. Grahovo (2000) is
famous for the great battles of 1861 and 1876.
Montenegro is an absolute hereditary monarchv, vested accord-
ing to the principle of primogeniture in the famUv of Petrovitch
Kyegush. ITie prince bears the title "Piince of Montenegro and
the Berda (mountains) " — Montenegro here meaning the old Mon-
tenegrin nahias (pi-ovinces) of Katunska, Tzrmitza, Eyetchka, and
' See Bogisii in Daa Austand, 187<.
Lyeshanska, and Berda the territory added in the 13th centciy,
OP the provinces Byelopavlitohska, Fiperska, Uoratcliska, Vasoye-
vitchska, and Kutska. A responsible ministry was introduced in_
1877, and there are now separate departments of justice, foreign ,
affairs, war, and finance and education. The highest adininistra-
tive body is the council of state, instituted in 1879, and consisting
of eight members appointed by the prince. Justice in ordinary
cases is rendered in primitive fashion. Formal codes were drawn
up by Peter I. (1798) and by Danilo (1855), but the real statu'-e
book is national custom. A great court, consisting of the minister
of justice, and five members named by the prince, is held in.th*
capital, and there are inferior courts in each of the captaincies
(86 in 1879). While formerly the very president of the senate, i
jlirko Petrovitch (o4. 1865), whose songs are the delight of hi*
countrymen, could neither read nor write, primary education has
been widely diffused during the reign of Prince Nicholas (Nikita.).
In 1851 there was only one school, but before the recent war they
had increased to 58, nearly every clan having one for girls as well
as for boys. The female itontencgrin Institute (founded and sup- '
ported by the empress of Russi.i) atti-acts pupils from beyond the
frontier. It was from the piiuting-presses of Cettinye and Ryeka
that the first books in the Slavonic languages were issued between
1483 and 1493, under the patronage especially of Ivan Beg and
George (IV.) Crnoyevitch, " waywodes of the Zeta," but this pro-
mise of literary productiveness 'was soon cut off by w^ars with the
Turks. Peter Petrovitch Nyegush (1813-1S51), who was called to
rule in 1830, is rec43gnized as perhaps the gi-eatest of all Servian
poets, — his Gorski Vii/cnac, or "Mountain Wreath," giving dramatic
expression to the " veiy soul of the Serbian people. Though the
press which he established in 1834 was destroyed in the war of
1852-53, another was soon obtained, and under Prince Nicholas,
himself a poet, his memory has proved a potent stimulus to
intellectual culture. The first Montenegrin newspaper, Cmogorac^
now Glas Cmogorca, began to appear in 1870 ; the first book-shop
was opened in 1879.-
The Montenegrins,' however, have had more to do with the
sword than with the pen. '* Every man, di-essed in the picturesque
costume of his tribe, carries his pistol and yataghan in his girdle."
NoniinaDy the age of military service is between si^cteen and
sixty-five, but when war- breaks out schoolboy and superannuated
veteran are equally eager for the fray. When Prince Nicholas tried
to prevent an old man of eighty from joining his forces, the insulted
warrior drew his pistol and shot himself. War Nvith the Turks,
indeed, is the essence of Montcnogiin history. On the death of the
Servian king Stephen Dushan, Prince Balsha became independent
lord of the province of the Zeta ; and when the Servian power
was shattered by the Turks in the battle of Kossovo (1389) his
territoiy formed the asylum of all those who deteimined to make
another stand for freedom. In 1485 Ivan Crnoyevitch', findini;
Zhabliak untenable, fixed his " capital " at Cettinye. In 1516 his
son George, who had succeeded him^ left his country to its fate ;
bat the people cho.se their bishop as their chief Prince-bishopa
or vladykas, elected by the people, continued to lead them with
success against the common foe of Chiistendom till 1697, when
the authority was handed over to Petrovitch Nyegush, with the
right of appointing his successors, subject to national approvaL
At length, in 1851, Danilo, nephew and nominee of the previous
vladyka Peter II., prevailed on the "skuptchina" to declare Mon-
tenegro a secular state with the hereditarj' government of a prince.
His nephew Nicholas succeeded to the throne in 1860, and at the
close of the war 1876-78 Montenegro was declared a sovereign
principality. For an account of the defeats and victories (the latter
by fai' the «iore numerous) which have marked the national straggle
for existen.:e during its fom- centiuies, the reader is referred to
Denton's Montenegro (Lond., 1877).
See Ohiervalion4 oil Monlejicffro (St Pet, 1831X by Baron Kaulbars, RoBSian
member of the IntematioDal Commission ; Willdnson's Dalmatia and Montentoro
(1818) ; Wlngdeld, Tour in Bn/malin, 4c. (1859) ; Viscountess Strangfoid, Tct
Eastern Shores of Iho Adriatic (.\S64}; A. J. Evans, Iltyrian Lettfre (1878) ; W. E.
Gladstune in the I^ineteentk Century, 1. ; Freeman, in Macmiltnn'e Mag., -1876 ;
Scliwarz, Moutencgro (1882). See also the bibliographies in 'BvU. de ta Soc. de
Ciogr. (Paris, 18C5) and ValentineUJ, Btb. della Dalnuuia (Agram, 1855).
(H. A. W.)
MONTEREY, a city of the United States, the capital
of California up to 1847, is situated on Monterey Bay,
125 miles south from San Francisco by the southern
division of the Southern Pacific Railroad. Originally
founded in 1770 as a mission station and presidio (garrison)
by Jvmipero Serra, it is still in the main a Spanish-looking
town, with Spanish talked in its streets and painted on its
signboards. At the meeting of the first constitutional
convention of California Monterey was a port of entry
with a flourishing trade and a promising future ; but it
soon suffered from the rivalry of San Francisco, and it i.s
Cf Pypin and Spasoritch, HUl. of Slat. Lileralures, voL t
782
M O N — M O I<
now a sleepy place, etraggling and dirty, vrith manj oi its
adobe b'lildings abandoned to decay. The flourishing Mon-
terey ■whaling company (chiefly Portuguese from the Azores)
has its station under the old tort ; and, the Southern Pacific
Railroad Company having erected (1881) a magnificent
hotel, the place bids fair to become cue of the leading water-
ing-places on the Californiau coast. The mission church of
Sail Carlos, aboul. four miles from the towTi, is a curious
and strildng ruin. Population is now (1883) about 1 tOO.
See Franc. Palou, V'ida del vm. padre fray J. Serra, Mexico,
1787; Lady Duffus Gordon, Through Cities and PrairU-lands,
1882 ; and Harper's Monthly Magazine, October 1882.
MONTEREY, a city of Mexico, capital of the state of
Nuevo Leon, lies 1600 feet above the sea on a sub-tributary
of the Rio Grande del Norte, 150 miles south-south-west
of Nuevo Laredo, and 190 west-south-west of Matamoras.
A handsome and well-planned city, with a cathedral and a
number of good public buildings, Monterey is also in com-
mercial and manufacturing activity the most important
place in the northern parts of the republic, and one of the
principal stations on the railway opened in 1882 between
the city of Mexico and the United States frontier (at
Matamoras and Nuevo Laredo). The population was about
37,000 in 1880. The city was founded in 1596, became
a bishopric in 1777, and was captured by the United
States forces under General Taylor in September 1846.
MONTE SAN GIULIANO, a city of Sicily, in the pro-
vince of Trapani and 12 miles north-east of the town of
Trapani, occupies the summit of the mountain from which
it takes its name. Rising in the midst of an undulating
plain, this magnificent aud conspicuous peak (the Eryx of
the ancients) hasj whether seen from sea or land, such an
appearance of altitude that, while it really does not exceed
2464 feet, it has for ages been popularly considered the
culminating point of western Sicily, and second only to
Mount Etna. By the Phoenicians it was early chosen as
the site of a temple, which continued down to the time of
the Roman empire to be one of the most celebrated of all
the shrines of Venus (Venus Erycina). The ancient city of
Eryx, situated lower down the mountain side, disappears
from history after the establishment of the Roman power
in Sicily, — the inhabitants having probably taken advan-
tage of the protection afforded by the sanctity, fortifica-
tions, and garrison of the temple-enclosure. In the modern
town, the population of which has recently decreased to
about 3000 by the migration of considerable numbers to
the plain, the chief points of interest are the cathedral,
internally restored in 1865, the castle, which occupies the
site of the temple, and the three so-called torri del Balio,
which probably represent the propylcea. Remains of
Phoenician masonry are still seen on the north side of the
town. The great rock-hewn cistern in the garden of the
castle is very like one of the cisterns of the Haram at
Jerusalem
The antiquities of Monto San Giuliano have been carefully in-
7estigated by 'Giuseppe Polizzi (/ Monmnenti d'Antichitd della
Provinda di Trapani), and by Professor Salinas {Archivio Storico
Sicilmno, L, &c.). Compare Ronan, Melanges d'Histoire et di
Voyages ; and Sayce in Academy, 30th December 1882.
MONTE SANT' ANGELO, a city of Italy in the pro-
vince of Foggia (Capilanata), 10 miles north of Manfre-
donia, stands on an oflshoot of Monte Gargano 2824 feet
high. In 491 the archangel Michael pointed out the
place to St Laurentius, archbishop of Sipontum (Man-
fredonia), and the chapel, which was built over the cave,
to which he drew more particular attention, soon became
a famous place of pilgrimage. Though plundered by
the Lombards in 657, and by the Saracens in 869, St
Michael's was already a wealthy sanctuary in the Uth
they are usually called) maintained a prolonged contest
with the Sipontino archbishops for episcopal independence.
According to Ughelli {Italia Sacra, vol. vli. p. 816),
a marble statue of the saint by Michelangelo Buonarroti
took the place of a tilver image. The bronze doors
still preserved are fine pieces of Byzantine work, made, as
^n inscription bears v,-itness, in Constantinople in 1076.
The town of Sant' Angelo, -which had only about 3000
inhabitant's in the 17th century, numbered 14,759 in 1861,
and 13,902 in 1871. Besides the festival of the saint
celebrated on the 9th of May, there is a great fair on the
29th of September.
MONTESQUIEU, Chasij:3 Louis de Seconbat,
Baeon de la Brisde et de (1C89-1755), philosophical his-
torian, was bom at the chateau of La Brfede, about 10 miles
to the south-east of Bordeaux, in January 1689 (the exact
date being unknown), and was baptized on the 18th of
that month. His mother was Marie Frangoise de Penel, the
heiress of a Gascon-English family. She had brought La,
Brfede as a dowTy to his father, Jacques de Secondat, a mem-
ber of a good if not extremely ancient house, which seems
first to have risen to importance in the early days of the 1 6th
century. The title of Montesquieu came from his uncle,
Jean Baptiste de Secondat, " president i mortier " in the
parliament of Bordeaux, — an important office, which, as well
as his title, he left to his nephew. Montesquieu was in his
youth knoT\'n as M. de la Brede. His mother died when he
was seven years old, and when he was eleven he was sent to
the Oratoriau school of JuUly, near Meaux, where he stayed
exactly five years, and where, as well as aiterwards at Bor-
deaux, he was thoroughly educated. The family had long
been connected with the law, and Montesquieu was destined
for that profession. He was made to work hard at it not-
withstanding his prospects (for his uncle's office was his by
reversion) ; but, as in his later life, he seems to have
tempered much study with not a little society. His father
died in 1713, and a year later Montesquieu, or, as he should
at this time strictly be called. La Brede, was admitted coun-
sellor of the parliament. In little more than another twelve-
month he married Jeanne Lartigue, an heiress and the
daughter of a knight of the order of St Louis, but plain,
somewhat ill-educated, and a Protestant. Montesquieu does
not seem to have made the slightest pretence of aflection or
fidelity towards his wife — things which, indeed, the times
did not demand ; but there is every reason to believe that
they lived on perfectly good terms. Like the three previous
years, 1716 was an eventful one to him ; for his uncle died,
leaving him his name, his important judicial oflace, and his
whole fortune. He thus became one of the richest and
most influential men in the district. He continued to hold
his presidency for twelve years, in the course of which he
had much judicial work to perform, as well as the nonde-
script administrative functions which under the old regime
fell to the provincial parliaments. He was none the less
addicted to society, and he took no small part in the pro-
ceedings of the Bordeaux Academy, to which he contributed
papers on philosophy, politics, and natural science. He
also wrote much less serious things, and it was during the
earlier years of his presidency that he finished, if he did not
begin, tho Lettres Persanes. They were completed before
1721, and appeared in that year anonymously, with Cologne
on the title-page, but they were really printed and published
at Amsterdam. This celebrated book (the original notion
of which is generally set down to a work of Duf resny,- the
comic author, but which is practically original) would have
been surprising enough as coming from a magistrate of the
highest dignity in any other time than in the regency of the
diie of Orleans, and even as it was it rather scandalized
century and its prosperity continued tiU the time of the the graver among Montesquieu's contemporaries. lu the
French' occupation. Tlie canons {Caiwnici Garganici, as I guise. of lettei-s written by and to two Persians of distinction
MONTESQUIEU
783
travelling in Europe, Montesquieu not only satirized un-
mercifully the social, political, ecclesiastical, and literary
follies of his day in France, but indulged in a great deal of
the free writing (so free as very nearly to deserve the term
licentious) which was characteristic of the tale-tellers of the
time. But what scandalized grave and precise readers
naturally attracted the majority, and the Lettres JPersanes
were veiy popular, passing, it is said, through four editions
within the year, besides piracies. Then the vogue suddenly
ceased, or at least editions ceased for nearly nine years to
appear: It is said that a formal ministerial prohibition
was the cause of this, and it is not improbable ; for, though
the regent and Dubois must have enjoyed the book
thoroughly, they were both shrewd enough to perceive that
underneath its playful esterior there lay a spirit of very
inconvenient criticism of abuses in church and state. The
fact is that the Lettres Persanes \a the first book of what is
called the Plulasophe movement. The criticism is scarcely
yet aggressive, much less destructive, and in Montesquieu's
hands it never became so ; but what it might become in
the hands of others was obvious enough. It is this pre-
cuisorship in his own special line which in all probability
made Voltaire so jealous of Montesquieu, as well as the
advantage which a wealthy and well-born noble of high
official position had over himself. It is amusing to find
Voltaire describing the Lettres as a "trumpery book," a
" book which anybody might have written easily." It is
not certain that, in its peculiar mixture of light badinage
with not merely serious purpose but gentlemanlike modera-
tion, Voltaire could have written it himself, and it is
certain that no one else at that time could. The reputa-
tion acquired by this book brought Montesquieu much into
the literary society of the capital, and he composed for, or at
any rate contributed to, one of the coteries of the day the
clever but rather rhetorical Dialogue de Sylla et cCBucrate,
in which the dictator gives an apology for his conduct. For
Mademoiselle de Clermont, a lady of royal blood, a great
beauty and a favourite queen of society, he wrote the
curious prose poem of the TempU de Gnide. This is half
a narrative, half an allegory, in the semi-classical or rather
pseudo^ilassical taste of the time, decidedly frivolous and
dubiously moral, but of no small elegance in its peculiar
style. A later jeu d'esprit of the same kind, which is almost
but not quite certainly Montesquieu's, is the Voyage d
Paphos, in which his warmest admirers have found little to
praise. In 1725 Montesquieu was elected a member of the
Academy, but an almost obsolete rule requiring residence in
Paris was appealed to, and the election was annulled. It is
doubtful whether a hankering after Parisian society, or an
ambition to belong to the Academy, or a desire to devote
himself to literary pursuits of greater importance, or simple
weariness of not wholly congenial work determined him to
give up his Bordeaux office ; it is certain that he continued
to hold it but a short time after this. It is tolerably clear
that he had already begun his great work, and the-character
of some papers which, about this time, he read at the Bor-
deaux Academy is graver and less purely curious than his
earlier contributions. In 1726 he sold the life tenure of his
office, reserving the reversion for his son, and went to live
in the capital, returning, however, for half of each year to
La Brede. There was now no further formal obstacle to his
reception in the Acad^mie Fran9ai3e, but a new one arose.
Ill-wishers had brought the Lettres Persanes specially under
the minister Fleury's attention, and Fleury, a precisian in
many ways, .was shocked by them. There are various
accounts of the way in which the difficulty was got over,
but all seem to agree that Montesquieu made concessions
which were more efiectual than dignified. He was elected
and received in January 1728. Almost immediately after-
wards he started on a tour through Europe to observe I
men, things, and constitutions. He travelled through
Austria to Hungary, but was unable to visit Turkey as he
had proposed. Then he made for Italy, where he met
Chesterfield. They sojourned together at Venice for some
time, and a curious story is told of the way in which either
a piece of mischief on Chesterfield's part, or Montesqviieu's
own nervousness and somewhat inordinate belief in his ow-a
importance, made the latter sacrifice his Venetian notes.
At Venice, and elsewhere in Italy, he remained nearly a
year, and then journeyed by way of Piedmont and the
Rhine to England. Here he stayed for some eighteea
months, and acquired an admiration for English character
and polity which never afterwards deserted him. He
returned, not to Paris, but to La BrMe, and to outward
appearance might have seemed to be settling down as a
squire. He altered his park in the English fashion, made
sedulous inquiries into his own genealogy, arranged an
entail, asserted, though not harshly, his seignorial rights,
kept poachers in awe, and so forth. Nor did he neglect
his fortune, but, on the contrary, improved his estates in
every way, though he met with much opposition, partly
from the dislike, of his tenants to new-fangled ways, and
partly from the insane economic regulations of the tim*j
which actually prohibited the planting of fresh vineyards.
Although, however, Montesquieu was enough of a grand
seigneur to be laughed at, and enough of a careful steward
of his goods to be reviled for avarice, by those of his con-
temporaries who did not like him, these matters by no
means engix)ssed or even chiefly occupied his thoughts.
In his great study at La Brede (a hall rather than a study,
some 60 feet long by 40 wide) he was constantly dic-
tating, making abstracts, re\ising essays, and in other
ways preparing his great book. Like some other men of
letters, though perhaps no other has had the experience in
quite the same degree, he found himself a little hampered
by his earlier work. He may have thought it wise to
soften the transition from the Lettres Persanes to the
Esprit des Lois, by interposing a publication graver than
the former and less elaborate than the latter. He had
always, as indeed was the case with most Frenchmen of his
century, been interested in ancient Eome and' her history ;
and he had composed not a few minor tractates on the
subject, of which many titles and some examples remain,
besides the already-mentioned dialogue on Sylla. All these
now took form in the Considerations sur les Causes de la
Grandeur et la Decadence des Romains, which appeared in
1734 at Amsterdam, without the author's name. This,
however, was perfectly well known ; indeed, Montesquieu
formally presented a copy to the French Academy. Anony-
mity of title-pages was a fashion of the day which meant
nothing. The book was not extraordinarily popular in
France at the time. The author's reputation as a jester
stuck to him, and the salons affected to consider -the Lettres
Persanes and the new book respectively as the " grandeur "
and the "decadence de M. de Montesquieu;" but more
serious readers at once perceived its extraordinary merit,
and it was eagerly read abroad. A copy of it exists or
existed which had the singular fortune to be annotated by
Frederick the Great, and to be abstracted from the Potsdam
library by Kapoleon. It is said, moreover, by. competent
authorities to have been tho most endm-ingly popular and
the most widely read of all it5 author's works in his own
country, and it has certainly been the most frequently and
carefully edited. Its merits are indeed undeniable. Merely
scholastic criticism may of course object to it, as to every
other book of the time, the absence of the exactness of
modem critical inquiry into the facts of history ; but thi^
is only a new example of a frequent ignoratio elenchi.
The virtue of Montesquieu's book is not in its facts but in
its -views. It is (putting Bossuet and Vico aside) almpsj
784
MONTESQUIEU
the first important essay in tb& philosophy of history.
The point of view is entirely different from that of Bossuet,
and it seems entirely improbable that Montesquieu knew
anything of Vice. In the Cj-and^r el Decadence the
characteristics of the Esprit des Loi« appear vnih the neces-
sary subordination to a narrower subject. Two things are
especially noticeable in it : a peculiarity of style, and a
peculiarity of thought. The style has a superficial defect
which must strike every one, and which was not overlooked
by those who v/ere jealous of Montesquieu at the time.
The page is broken up into short paragraphs of but a few
lines each, which look very ugly, which irritate the reader
by brealdng the sense, and which prepare him to expect
an undue and ostentatious sententiousness. The blemish,
however, is chiefly mechanical, and, though no editor has
hitherto had the perhaps improper audacity so to do, it
would be perfectly possible to obliterate it without changing
a word. On the other hand, the merits of the expression
are very great. It is grave and destitute of ornament, but
extraordinarily luminous and full of what ■would be called
epigram, if the word epigi'am had not a certain connotation
of flippancy about it. It is a very short book ; for, printed
in large type with tolerably abundant notes, it fills but
two hundred pages in the last edition of Montesquieu's
works. But no work of the centiu-y, except Turgot's second
Sorbonne Discourse, contains, in proportion to its size,
more weighty and original thought on historical subjects,
while Montesquieu has over Turgot the immense advantage
of style.
Although, however, this ballon d'essai, in the style of his
great work, may be said to have been successful, and though
much of that work was, as we have seen, in all probability
already composed, Montesquieu was in no hurry to publish
it. He went on " cultivating the garden " diligently both
as a student and as an improving landowner. He had
lawsuits, sometimes on his own account, sometimes on that
of others, and in one case he vpon from the city of Bordeaux
BO less than eleven hundred crpents of, it is true, the un-
productive landes of the country. He is said to have
begun a history of Louis SI., and there is a story that it
was completed but burnt by mistake. He -wrote the
sketch of Lysimaque for Sunislaus Leczinski; he published
new and final editions of the Temple dc Guide, of the Leitres
Persanes, of Sylla et Eucrate {vihich. indeed had never been
published, properly speaking). After allowing the Grandeur
et Decadence to be reprinted without alterations some half
dozen times, he revised and corrected it. He also took
great pains with the education of his son Charles and his
daughter Denise, of whom he was extremely fond. He
frequently visited Paris, where his favourite resorts were
the salons of Madame do Tencin and Madame d'Aiguillon.
But all the time ho must have been steadily working at
hia book, indeed, a contemporary accuses him of having
only gone into society to pick up materials for it. But it
aeems that he did not begin the final task of composition
till 1743. Two years of uninterrupted work at La Brfede
■finished the greater part of it, and two more the rest. It
was finally published at Geneva in the autumn of 1748, in
two volumes quarto. The publication was, however, pre-
ceded by one of those odd incidents which in literature iUus-
trato Clive'a well-known saying about courts-martial in war.
Montesquieu summoned a committee of friends, according
to a very common practice, to hear and give an opinion
on his work. It was an imposing and certainly not an
unfriendly one, consistingof H^nault, Helvdtius, the financier
Silhouette, the dramatist Saurin, Cribillon the younger,
and lastly, Fontenelle, — in fact, all sorts and conditions
of literary men. The members of this eminently competent
tribunal unanimously, though' for different reasons and in
different forms of expression, advised the author not to
publish a book which has been recently described by \-
judge of certainly not less competence as "one of the most
important books ever written," and which, when importance
of matter and excellence of manner ai-e jointly considered,
may be almost certainly ranked as the greatest book of
the French 18th century.
Montesquieu, of course, did not take his friends' advice. In
such cases no man ever does, and in this case it was certainly
fortunate. The Esprit des Lois represents the reflexions
of a singularly clear,, original, and comprehensive mind, cor-
rected by forty years' study of men and books, arranged in
accordance with a long deliberated plan, and couched in
language of remarkable freshness and idiosyncrasy. The
title has been somewhat cavilled at, and, like that of the
Considerations, it gave a handle to the somewhat maliciou
frivolity of the salons. But if it had besr. jjreserved i'
full it would have escaped much of the criticism which i :
has received. In the original editions it runs L'Espril
des Lois : ou du Rapport que les Lois doivent avoir avec la
Constitution de chaque Gouvemement, les M<evrs, le Climat,
la Beligion, le Commerce, etc. It consists of thirty-one
books, which in some editions are grouped in six parts. This
division into parts is known to have entered into the
author's original plan, but he seems to have changed hLs mind
about it. Speaking summarily, the first part, containing
eight book's, deals mth law in general and with ' forms of
government ; the second, containing five, with military
arrangements, with taxation, &c. ; the third, containing six,
with manners and customs, and their dependence on
climatic conditions ; the foiulh, containing four, with eco-
nomic matters ; and the fifth, containing three, with religion.
The last five books, forming a kind of supplement, deal
specially with Eoman, French, and feudal law. The most
noteworthy peculiarity of the book to a cursory reader lies
in the section dealing with effects of climate, and this
indeed was almost the only characteristic which the vulgar
took in, probably because it was easily susceptible of
parody and reduciio ad absurdum. But this theory fa
but the least part of the claims of the book to attention.
Its vast and careful collection of facts, the novelty and
brilliancy of the generAliaatioos founded on them, tha
constructive spirit which penetrates it, its tolerance, ita
placid wisdom lighted up by vivacious epigram, could only
escape the most careless reader. The singular spirit of
moderation which distinguishes its views on politics and
religion was indeed rather against it than in its favour in
France, and Helv6tins, who was as outspoken as he waa
good-natured, had definitely assigned this as the reason of
his unfavourable judgment. On the other hand, if nol
destructive it was sufiiciently critical, and it thus raised
enemies on more than one side. Montesquieu was thought
too English in his ideas by some, the severe defenders
of orthodoxy considered him latitudinarian, and one
zealous Jansenist informed him that he was "a pig."
It was long suspected, but is now positively known, that
the book (not altogether with the goodwill of the pope)
was put on the Index, and the Sorbonne projected, though
it did not carry out, a regular censure. To all those ob-
jectors the author replied iu a masterly defense; and
there seems to be no foundation for the late and scandalous
stories which represent him as having used Madame de
Pompadour's influence to suppress criticism. The fact
was that, after the first snarlings of envy and incompetence
had died away, he had little occasion to complain. Even
Voltaire, who was his decided enemy, was forced at length
to speak in public, if not in private, compliinentarily of the
Esprit, and from all parts of Europe the news of succeds
arrived.
Honteaquieu.enjoyed his triumph rather at La Bride than
at Paris. He was becoming an old man, find, unlike Fonte-
I
J
M O N — M O IS
785
nelle, he docs not seem to Lave preserved in old age the
passion for society which had marked his youtli. A ratter
dubious description, published long after his death, repre-
sents him as '• wandering in his woods from mom to night
with a white cotton niglitcap on his head, and a vine prop
on his shoulder." Tliis, in the fiorid langixage of us tiine
(the Eepublicci!! periocJ), is probably oniy an in:a£inative
exprcJaiou of h\r, kno^rn interest in managing his estate.-
But he cejir.inly spent much of his later years ia the
country, though ha sometimes visited Paris, and on one
visit had the tipportunity, which he is likely to have en-
joyed, of procuring the release of his admirer La Beaumclle
from an imprisonment which La Beaumelle had suffered
at the instance of Vdtairo. Ho is said also to have been
instrumental in obtaining a pension for Piron. Indeed,
indigent or unlucky men of letters found in him a constant
protector, and tiiat not merely at the royal expense. Nor did
he by any means neglect literary compoj-ition. The ciirious
little" romance of Arsftic el hmenit, a iiliort and unfinished
treatise on Taste, many of his published Pensces, and much
unpublished matter date from tiis period subsequent to
the Esprit dis Lois. He did not, however, live many years
after the appearance of his great work. At the end of
1754 he visited Paris, with the mtention of getting rid of
the lease of his house there and finally retiring to La
Bride. He was shortly after. taken ill with an attack of
fever, which seems to hare affected the lungs, and in less
than a fortnight he died, on 10th February 1755, aged
sixty-sis. He was buried in the church of Saint Sulpice
with little pomp, and the Revolution obliterated all trace
of his remains.
The literary and phupsopMcal merits of Montesquieu and his
position, actual and historical, in the literature of France and of
Europe, form a subject of rather unusual interest in its kind. At
the beginning of this century the vicomte de Bonald classed hiui
with Raciuo and Bossuet, as the object of a "religious veneration"
among Frenchmen. But Bonald was not quite a suitable spokes-
man lor France, and it may be doubted whether the author of the
Esprit des Lois lias ever really occupied any such position in his
own country. For a generation after nis death he remained indeed
the idol and the great authority of the moderate reforming party
in France, and at such times as that party recovei-id power during
the revolutionary period Montesquieu recovered vogue with it
But the tendency of the centnry and a quarter which have passed
•ince his death has been to reduce the numbers and position of
this parly ever n.ore and more, and Jlontesquieu ia not often qnot-
able, or quoted, either by Kepublicans, Bonapartists, or Legitimists,
at the present day. Again, his serious works contain citation of or
allusion to a vast number of facts, and the exact (let it be hoped
that posterity will not call it the pettifogging) criticism of our
time challenges the accuracy of these facts. Although he was
i-cally the founder, or at least one of the founders, of the sciences of
comparative politics and of the philosophy of history, his descend-
ants and followers in these aciences think they have outa-OH-n
him. In France his popularit}' has always been dubious and con-
tested. It is a aingatar thing that, uutil within the last decade,
there has been no properly edited edition of his works, and nothing
even approacliing a complete biography of him, the place of the
latter being occupied by the meagre and rhetorical Elorjcs of the
last century. Ho is, his chief admii-crs assert, hardly read at all
in Fiance to-day, and a tolerable familiarity with modem French
literature enables its possessor to corroborate this by first-hand
knowledge, to the effect that no writer of equal eminence ia so little
quoted. The admirers just mentioned attempt to explain '.he fact
by confessing that Montesquieu, great as he is, is not altogether
great according to French principles. It is not only tliat he is an
Anglo-maniac, but that he is rather English than French in style
and thought. His work, at least th". Esprit, ie lacking in the pro-
portion and the al:nost ostentatious lucidity- of arrangement whicl'.
a Frenchman dem.-.nd.^. His sentences are often enigwatica!, and
!u;;gestlve rather than clear. He is alnicst entirely dUpa.'ssiouate in
politics, but he laclcs the unsM-ernng deducrive consistency which
ii'cnchmen love in that science. His wit, it is said, is quaint and
a little provincial, his style irregular and in no definite genre,
Some of those things may be allowed to exist and to be defects
in Montesquieu, hut they are balanced by merits which render
tliem almost insignificant. Of the mino; works, which are on the
T*bolt' rather unworthy of their author, nothing need be ssid here.
scattered about the tolerably numerous letters which have reached
us, tliere is much acnteness and point, as also in some of the best
sentences of the CmiMcUralimis and of t:;e EspriL But no one would
put Montesquieu as a pensh, or maxim, writer beside La Roche-
foucauld and Joubevt, Pascal and Vauvenargues. It is on his thice
princijjal works that his fame does and must rest Each one of
these IS a masterj.icce in its kind. It is doubtful whether tiie
LeUrts Fcrsanes yield at their best either in wit or in giving lively
pictures of the time to the best of Voltaire's similar work, though
they are more unequal. There is, moreover, the great difference
between Montesquica and Voltaire that the former is a rational
reformer, and not a mere pcrsijlextr or frcnidciir, to whom fault-
finding is more convenient for showing off his wit than acquiescence.
Of course this last description does not fully or always describe
Voltaire, but it often does. It is seldom or never applicable to
Jlontesquieu. Only one of Voltaire's own charges against t.c:
book and its author must be fully allowed. He is said to hr,' ■!
replied to a friend who urged him to give up his habit of sneer! x
at Montesquieu, **il est coupable de lese-poesic," and this is triii-.
Not only are Montesquieu's remarks on poetry (he himself occasiou-
ally MTote verses, and veiy bad ones) childish, but he is never happy
in purely literary appreciation. The Considiralions arc notowortb y.
not only for the complete change of style (which from the light anii
mocking tone of the Letlrt$ becomes grave, weighty, and sustaincil.-
mth abundance of striking expres-sion), but for the profundity aiid
originality of the views, and for the completeness with which tho
author carries out his plan. These words — except, perhaps, the last
clause — apply with increasing force to the Esprit des Lois. 'The book
lias been accused of desultonness, but this arises, in part at least,
from a misapprehension of the author's design. At the same time,
it is irapossible to say that the equivocal meaning of the word ' ' law,"
wliioh lias misled so many reasoners, has not sometimes misled
Jlontesquieu himself For the most part, however, he keeps tl'.e
promise of his sub-tit'e (^vcn above) with fidelity, and applies it
\rith exhaustive care. It is only in the last few books, which hove
been said to be a kind of appendLx, that something of iirelevancy
suggests itself. The real inipoitance of the Esprit dcs Lois, how-
ever, is not that of a formal ti-eatise on law, or even on polity. It is
thatofanassemblageofthemostfeitile, original, and inspiritingvicv. 3
on legal and political subjects, put in language of singular suggc'i-
tiveness and vigour, illustrated by examples which are always a',t
and luminous, permeated by the spirit of temperate and tolerant de-
sire for human improvement and happines.*?, and almost unique i.i
its entire freedom at once from doctrinaiiiauism, from visior.aiy
enthusiasm, from egotism, and from an undue spirit of syste;ii.
As for the style, no one whc does not mistake the definition of th.t
much used and much misused word can deny it te Montcsqoieti.
He has in the Esprit little ornament, but his composition is whohy
admirable. Every now and then there are reminiscences, perhaps :t
little mor« close than is necessary, of the badinage of the Lettres hr-
sanes, but these are rare, and the author's wit is for the most nscd
only to lighten his pages. Yet another great peculiarity of this book,
asveMoisoltheConsid^ratioiis, has to be noticed. The genius of the
author for generalisation is so great, his inr.tiuct in political science
so sure, that even the falsity of his premises frequently fails to
vitiate his conclusions. He has known \Tong, but he has thought
The 8»le ed'rtion cf Montesquieu which nceJ be mentioned here is that kX
Edouaid Laboukye (7 vo!i., Parle, 1S75-187C). the sole biography that of Lcii^s
Viao (Paris, necond cditioii, ISTD). From the titter the tacts of the above not.-i;
are principally drawn. The bibliography of Montesquieu's published woi^k*
is not of auy special interest, but in resjiect ot anecdota he occupies a singul.lr
position. Theto is known to exist at La Brede a great mass of IISS. matenils
tor the EspHl da Lois, additional LcUris Ptrsuitci, essays and fragme-Jto i..
ell kinds, diaries, letters, notebooks, and so forth. The present possessors,,
however, who represent Montesquieu, though not in the direct male line, lu^o
hitherto refused pei-miision to examine these to all editors and critics. thoii;.U
the publication of some of them has been vaguely promised. At present Ui'-/
ara chiefly kno»-n by a paDer contributed nearly halt a century ago to tlio
Tmnxicticas of the Academy of Agen C1S3-0- C^' E-^)
MONTEVERDE, Clatoio (15681643), the invent :r
of the " free style " of musical composition, was born at Ci'. -
mona in 1568; he was engaged at an early age as vioUt
to the duke of Muutua, and studied composition with ton.o
success under Ingegneri, the duke's "maestro di cape!!;i,'^
though without thoroughly mastering the difficulties of
mu-'iical science. His knowledge of counterpoint was limittd.
and his ear imperfect, but he was a bold experimenter, and
his undisguised empiricism led to discoveries which exercised
a lasting influence upon the progress of art. He was the
first composerwho ventured to use unprepared dissonances, —
employing them first in his madrigals, the beauty of which
they utterly destroyed, but afterwards introducing them
into music of another kind with such excellent effect that
their value was universally recormized, and all opposition
tT 1'. ■■;• i;-,.- t'^-_'-::.!!v ;.:'!;r.;id. In 1G03 he succeeded
Iti— 2?>
786
M O N — M O N
Ingegneri as "maestro di capella ;" and in 1 C07 lie produced,
for the marriage of Francesco Gonzaga, -'^'''-^'■st opera,
Ariana, in -n-hich he employed the newly-diSCOveud dis^
cords v.-ith irresistible effect. Though he did not invent the
lyric drama — Peri's Enridice having been produced at
Florence in 1600 — he raised it to a level which distanced
all contemporary competition. ' His second opera, Orfeo,
composed in 1608, was even more successful than Ariana,
and was based upon a principle which is held by some
modern critics to embody the only law to which the
dramatic composer owes obedience — that of accommodating
the music to the exigencies of the scene. In 1613 Monte-
verde was invited to Venice, as " maestro di capella " at St
Mark's. Here he composed much sacred music, the gTeater
jiart of which is lost, — acircumstance the less to be regretted,
since his Ycqiers and 2Iasses bear no comparison with thdsn
produced by his predecessors in ofHce. In 1630 he wrote
another grand opera, Proserpina rapita. In "1639 he pro-
duced L'Adcne, and in 1 641 Ze Ifozse di Enea and // ritorno
dUli^se. These later works show him still greatly in
advance of his age, notwithstanding the progress made by
other composers since the production of Orfeo. Jlonteverde
was ordained priest in 1633; and he died in. 1643, uni-
versally respected. Though his free emploj-ment of the
dominant seventh and other unprepared discords put an
end to the school of Palestrina, it led the way to the greatest
achievements of modern music.
MONTEVIDEO, S.vk Felipe y Santiago de, the capital
of the republic of Uruguay (Banda Oriental) in South
-America, lies on the eastern side of a nearly semicircular
bay on the northern shore of the estuary of the La Plata,
120 miles from Buenos Ayres, with which communication
is maintained by a daily service of steamers. The small
peninsula on which the city is built does not rise more
than 95 feet above the level of the sea ; but the headland
of Cerro, 505 feet high, whic'u forms the western side of
the bay, is notable enough on that low-lying coast to justify
the name Montevideo ; it is cro\vned by a lighthouse,- and
by an old Spanish fort, once of considerable strength. About
620 acres is the area occupied by the. city proper; the
suburbs stretch for miles into the country. The plan both
of the old and the new to^^•n is regular ; they are separated
by the Calle de la Ciudadela on the line of the old ramparts.
A somewhat Oriental appearance is produced by the low
houses with their flat terraced roofs and miradors or watch-
towers, from which the merchants look out for ships. As
a whole, the city is overbuilt, and immense wealth has been
squandered in Italian marbles and other forms of archi-
tectural decoration. The streets are for the most part well
])aved, and there is an extensive tramway system. Mare's
grease was for some time employed to make gas for light-
ing ; but an epidemic having commenced at the gas-yard
the woiks were for a timo closed, and when they were re-
opened coal-gas was suljstituted. Previous to 1870, when
water was introduced from a distance of -10 miles, the whole
supply was dependent on the rainfall. In the old town
the i)rincipal s.quaro is the Plaza de la Constitucion, the
south side of which contains the "cathedral," and the north
side the caUldo (law-courts, senate-house, and prison). The
cathedral (as it is usually called, though tlie bishop is a
bLshop in jMrtihw, and takes his title from Megaera in Asia
Jlinor) is a somewhat imposing building, consecrated 21st
October 1804, with a dome and two side towers 133 feet
liigli, which forra.one of the best landmarks of the bay. In
the line of the old ramparts formerly stood the old Spani.sh
citadel, which was built by the seven years' forced labour
of 2000 Guarani Indians. From 1835 to 1868 it served as
tho'piincipal market in the city; in 1877 it was removed
aitd the area vinited with the fine Plaza do la Independencia
at fiat south-western end of the Calle del 18 Julio, a broad
street which runs in a straight lino right through the n' .v
town. The new market, covering 2 acres, was built iu
ICoJi «t a cost of £86,000, and there are besides the Port
market (cost £55,320) and the Mercado Chico. The ex-
change, constructed after the style of the house at Bordeaux,
dates from 1864, and cost X32,000. Of note also are the
custom-house, the post office (1866), the museum, the public
library (founded in 1830 by Dr J. M. Perez Castellano), the
university (dating from 1849), the Soils theatre (1856), the
British hospital (established in 1857, present building 1867),
the Hospital de Caridad (founded by Francisco A. Macil in
1825), having an average of 300 patients, the new lunatic
asylum (1877), the Basque church (1858), and the English
church (1845), buUt on the site of a battery taken in 1807
by Sir Samuel Auchmuty'a forces. Since the beginning of
Map of MoDtevIdeo.
the century the depth of water in the bay has been allowed
to diminish 5 feet, and the area has been reduced by the
construction (1868) of an embankment to carry the railway
across it. Dredging has been tried from time to time, but
on too limited a scale. "The so-called harbour is a space of
less than half a mile square off the north-west face of the
tawn ; in 1 870 it was reported to be yearly becoming smaller
and less safe, and vessels are now obUged to anchor farther
out. Among modern improvements in the port the most
noteworthy are the Maua dry docks, -opened in 1873, and
the larger docks, erected in 1877 at a cost of 2,0,00,000
dollars, at the foot of the Cerro on the other side of the
bay. The trade of Montevideo consists mainly in the ex-
port of the raw products of the slaughter-house (horns,
hides, hair, tallow, wool, bones), with a certain quantity of
live stock and preserved meat, and in the import of European
manufactures. Duringthe five years 1877-1881 theayerage
value of the exports was £2,303,061, and that of the imports
£3,469,997. Of the 1044 vessels (tonnage 780,870) Avhich
entered in 1879, 285 were English, 157 Spanish, 145 Italian,
112 German, and 99 French. The population is large!)- of
foreign origin, Italian, Spanish, Basque, and French. In
1874 the Italians, who had rapidly increased after tho
siege, were about 40,000 strong, and in several quarters of
the city nothing was to be heard save Korth-Italian dialects
Even in 1880, after the e.xodus caused by the confiscations
of 1875, they numbered 36,300. The greater proportion
are engaged as petty traders. In 1879 the total population
of the town was 73,879 ; it had been 92,260 in 1878, and
105,296 in 1871, and now (1883), including the environs,
is 110,167.
Moutcvifico owes its origin not to tho commercial advantages
C'T its position but to the jealousy of the Spaniards towards the
Portuguese, which led Zabala, viceroy of Buenos AjTes, to erect a
fort at tills iioint in 1717. In 1726 the fii-st settlers were intro-
duced from liio Canary Islands aud Andalusia, aud more than fifty
M 0 N — M 0 N
787
^eara passed before the settlement was declared a port ; but by
1781 it had 6460 inhabitants, and by 1702 vras iini»orting to the
value of 2,993,267 dollars, and exporting to the value of 4,150,523.
In 1803 the governor of Montevideo was the first to revolt against
the Spanish authoiities, and to establish an independent junta ;
twenty years later, after nruch disastrous confusion and conflict, the
city became the recognized capital of the newly- formed republic
of Banda Oriental. Its population, which had been about 36,000
st the opening of the century, was reduced to 9000 by 1829 ; and
it had hardly recovered its ground in this respect (31,189) when,
in 1813, Rosas, dictator of Buenos Ayrea, wishing to compel annexa-
tion to Buenos Ayres, commenced the siege which was irregularly
maintained till 1852, and left the city and the country exhausted
and almost mined, .By 1860, however, the population had in-
crcns^-d to 49,548 ; and though the BraEilians blockaded the port
in 1504-5 and reinstated ex-president Flores the prosperity of the
place was but little impaired. During the Paraguayan war, which
lasted till 1864, Montevideo grew rapidly rich, attracting a large
sli.ire of the ti-ado diverted from Buenos Ayres. Immigrants
flocked from all quarters, and excessive investments were made in
all kinds of real property. The valuation of the city and suburbs,
which v.-as 14,156,000 dollars in 1860, reached the sum of
74,900,000 dollars in 1872. Reckless speculation, political dis-
sension, and the financial mismanagement of the Government have
told heavily ; the vahie of house property has greatly diminished,
and commercial activity has been giievously restiicted. Since 1 881 ,
however, Montevideo has been lupidly recovering, and its natural
advantages are so great that, with better political circumstances,
a future of yet higher prosperity may be anticipated.
N'otius of Montenileo will be found in BoneDi, TrxtveU in SoUvia, 4c., 1854 ;
Hadfleltl, Brasil, Vu Siver PiaU, 4c., 1S5-I, and his supplemental volnme, 1868 ;
Mulhalt, Handbook of thi River FlaU Mepttbties, 1S74; and Gallenga, South
Anrrica^ 1S81. See also Brignardello, Dclle vicejide tUW America merid, e
tpeeialm. di ilonteviJco nelV Vruguaij, Genoa, 1873 : Tk« Republic of Urvgiiay,
18S3 ; the reports of the municipal junta, and VallUnt's statistical publications,
MONTEZUMA. See Coktes and ilExicx*
MONTFAUCON, Beknaed de (1655-1741), critic and
Scholar, was bom of a noble and ancient family at the
chateau of Soulage (now Soulatgi, in the department of
Aube, France), on 13th January 1655. Though destined for
the army, he passed most of his time in the library of the
castle of Roquetaillade (the usual residence of his family),
devouring books in different languages and on almost every
A-ariety of subject, his studies being directed by a learned
friend of his father, Pavilion, bishop of AJeth. In 1672
he entered the army, and in the two following years served
as a volunteer in Germany under Turenne. But ill-health
and the death of his parents brought him back to his
studious life, and irt 1675 he entered the cloister of the
Congregation of St Maur, at La Daurade, Toulouse, taking
the vows there on 13th May 1676. Apart from his vast
literary labours, the remainder of his life presents little to
record. He lived successively at various abbeys — at
Soreze, where he specially studied Greek and examined
the numerous JISS. of the convent library, at La Grasse,
and at Bordeaux; and in 1687 he was removed to Saint
Germain des Pres. From 1698 to 1701 he lived in Italy,
chiefly in Rome. Returning to Saint Germain, he was
made a member of the Academie des Inscriptions et Belies-
Lettres in 1719. He died on 21st December 1711.
His fii-st publication, in which he was assisted by I^pia and
Pouget, was the first volume of a never completed series of previously
unpublished Annlcda Grxca. (168S). In 1690 appeared Lis defence
of the literally Ivistorical cliaracter of the book of J udith. Athaiiasii
oycra omnia, still the best edition of that father, was issued with
a biogi^pliy and critical notes in 1598. The first-fruits of his visit
to Italy were seen in his copious Diarium ItctHcum, sin moiiumcn-
toritm vctcrum, bibliothecannn, mHsaeorum, d:c., notitim singulares
in itinerario Ilalico collcda (1702). The Palmographia Grmca,
site de orttt cl progrcau literarum Grmcarum, et dc variis omnium
ssecttlorum scriptionia Ctxcs: generibus (1708) is a standard work,
which has not yet been superseded ; in its own field it is as original
as the De re diplomalica of ^lablllon. In 1713 ilontfaucon edited
Hexaphrum Origenis qus snperstmi (2 vols, fol.), only recently
superseded by the work of Field ; and between 1718 and 1738 he
completed his edition of Joannis CKrysosiomi opera omnia (13 vols,
fol.), which is hardly an improvement upon that of H. Saville. His
VAntiquiU cxpUqnfe et representee en figures (10 vols, fol., 1719)
would of itself suffice to establish a reputation for colossal dili-
gence. It was continued by him in Lcs Monxonens dc la ilojiarchie
Frartfoiae (5 vols..fol., 1729-1733). A complete list of his literary
iabouis, including his numerous contributions to the Mtmoircs of
the Academy of Inscnptions, will be found in the NouvcUe Bic-jraphit
G^nirah, 6. v. V Jlontfaucon. "
MONTFOET, SiMo.v de, Eael of Leicester (c. 120O-
1265), a great political leader, and sometimes even re-
ferred to as the " founder of the English House of Com-
mons," born in France about the beginning of the l.'ilh
century, was the fourth and youngest son of Simon IT.
de Montfort and of Alice de Montmorency. Of his early
life and education nothing is known, the first definitely
recorded fact about him being that in April 1230 he wa.s
in England and had attached himself to the service of
Henry III., who granted him a temporary pension of 400
marks, with a promise of the earldom which his father had
held.' In the following year he did homage for the
honour of Leicester, and in 1232 the king confirmed to
him all the land with appurtenances which had belonged
to the late earl in England. But, though thus formally
admitted to the ranks of the English baronage, he did not
for several years succeed in making way against the strong
dislike in which "aliens" were now held, and until 1230
most of his time was spent, in considerable povertyj
abroad. In that year, however, he attended the king's
marriage to Eleanor of Provence as lord high steward,
and thenceforward began to take part in the business of
the royal council. Handsome, talented, and brave, he
gained the love of Eleanor, widow of the earl of PembroVe,
and sister of the king, to whom he was privately married
at Westminster on 7th January 1238, Henry himself
giving away the bride. When the fact became known,
the indignation of the baronage and of the people had
almost broken out in open rebellion, and, after Simon had
with difficulty averted this by propitiating his brother-
in-law, Richard, earl of Cornwall, he found it necessary to
go to Rome to meet the objections which the church had
raised on the ground of an alleged previous vow made by
Eleanor. Having succeeded in obtaining (by bribery, it
would seem) the papal sanction to his marriage, he re-
turned to England in October, and early next year, still
in the enjoyment of the royal favour, he had the earldom
of Leicester formally conferred upon him in presence of
the assembled barons. In June (1239) he assisted as god-
father and high steward at the baptism of Prince Edward ;
but the machinations of his enemies were soon afterwards
successful in bringing about a change in the fickle humour
of Henry, and when Simon came back to Westminster id
August to attend the churching of the queen the king
met him with the information that he was an excommuni-
cated person, and ordered him to leave the church.'- Along
with his wife he forthwith went into volvmtary exile in
France; but in April 1240 he returned to England, and
was received by the king on a footing of at lea-st outward
friendship. Of his private and public life during the
' Simon IV. de Jlontfort, the welI-knoi\-n Albigsnsian crusa<i<;r, in
right of liis mother, Amicia de Beaumont, sister and co-helress of Robert
Fitz-Peruell, earl of Leicester, succeeded to that earldom in 1204, and
in 1207 W.13 confirmed in the liigh stewardship of England, hereditary
iu connexion with the title. Soon afterwards he was deprived of his
English possessions under some pretext, the real reason doubtless
being his position as captaiu-general of the French forces against the
Albigenses (1208). He received4hem again towards the end of John'*
reign, their custody, however, being committed to his nephew, the eail
of Chester. The long hostility between England and France during
the early years of Heury III. made it practically impossible for the
alien De Montforts to maintain any hold upon their English earldom
on the death of Simon IV. in 1218 ; in 1231, after the peace, the
eldest son Aniaury (now constable of France) renounced all claim t'r
it, thus learing the field clear to his next soniving brother Simon.
' There is no evidence that Simon actually had been excommuni-
cated, but it seem', ripar that certain payments he had agieed to make
to the Koman ciir'ia had not been punctually attended to, aud that
some anncvance had bem in this way caused to the king. The charge
of immorai relations with Eleanor was probably only a conveniently
coarse way of restating the ecclesiastical offence for which Do Mont-
fort had already purchased absolution.
788
O JS — M O N
next eight years Toiy few facts have been preserved.
There is soms ground for bcheving that he n-ent to the
Holy Land '}n 1240. and a letter ia still extant in which
the nobility of the kingdom of Jerusaler;-! ask Frederick
n. (June 1241) to allow Simon de Montfort, earl of
Leicester, to act as regent tiU the arrival of his son Conrad.
In 1242 ho accompanied Henry's unsucccsEful expedition
to France. In the parliamentary history of these years
his name appears but seldom, but -where he is mentioned
he is invariably found on the side of the people, resisting
alike the arbitrary wastefulness of the kijig and the
rapacious exactions of the pope. In 1248 Do Montfort
was appointed for six years the king's "seneschal," or
"locum-tenens," in Gascony. In this capacity he was
very inadequately supported from home with either men
or money ; he more than once subdued the rebellious
provinces, indeed, but meanwhile his enemies at home
gained strenjjth and encouraged the Gascons in repeated
accusations and complaints against the seneschal. These re-
sulted in one-sided inquiries; but ultimately in his acquittal,
and led to a demand on his part for reparation, and a con-
sequent quarrel with the king. Towards the end of 1252
De Montfort reth'ed into France, where such was the
reputation he enjoyed as a statesman that, on the death of
the queen-regent and in the absence of Louis IX., he was
offered the office of high steward and a place among the
guardians of the crown. This, however, he declined, " being
unwilling to prove a renegade;" and, after a partial recon-
ciliation with Henry, he retmmed to England in 1254. In
the foUowLag year he was sent on a secret mission into
>Scotland, and in 1257 he was one of the king's ambassadors
to France; but his chief activity between 1254 and 1258,
if wo are to judge by the prominent place he took in the
revolution of the last-named year, must have been in the
meetings of parliament. At the Westminster parliament
in April 1258' it was significantly upon the earls of Glou-
cester and Leicester that the king's half-brother, William
de Valence, laid the blame of all the evils under which the
country was groaning, De Montfort in particular being
called by liim " an old traitor and a liar." At Leicester's
suggestion the barons leagued for the defence of their
rights, and presented themselves armed at the meeting,
which extorted the appointment of the committee of
twenty-four to meet at Oxford and proceed at once with
tlie reform of the realm. The Provisions of Oxford having
been signed (October 1258), De Montfort received the cus-
tody of the castfe of Winchester, where the parliament con-
tinued its session, ho meanwhile apparently holding the
position of military commander4u-chief ; and, after the
removal of the barons to London, he was appointed member
of an embassy to Scotland. In the early part of 1259 he
was chiefly busied with the task of adjusting the terms of
a peace with France, which was not settled until the end of
that year. From the date of .the conclusion of that peace,
owing to divisions in the reforming party, the king began
■to regam liis lost power, and in 1262 he felt himself strong
enough to repudiate the Provisions of Oxford, thus giving
the signal for civil wa,r. The successes of the barons, led
by De Montfort, in the west, and his victorious entry into
London .again reduced the king to submission, but only to
bring once more also into prominence the divided slate of
Lticcstcr'a supporters. Louis's one-sided Mise of Ajr.iens
(1204), however, rendered another appeal to arms on the
;;art of the bai-ons inevitable, and by the victoiy of Lewes
(14th May 12G4) Do Montfort for the time became master
of England. Taking Hemy, his prisoner, along v/ith him
to London, he summoned thither the parliament, which
met in June, and drew up the constitution or scheme of
government a-scocialcd with his name, of which the most
utrikuig feature is the new development it gives to the
representative ayslcra. A .".till further adv^iicc in the
development louk place in 1265, when borough member.;,
as distinguished from county members, were for the first
time summoned. Mciv.vhile troubles in the west required
De J!ontfort'.s presence in the field, and, by tlie alliance of
his rival Oloucej.ttr wii,h Roger Mortimer, as well as by
the escape of Prince Edward, who put himself at the hea<l
of the royalist opposition, the great parliamentary leader
was placed in serious .-straits. At Evesham, where he had
halted on his march to join his son at Kenilworth, he was
surprised by the army of Prince Edward, and after •
struggle of about two hours was slain on the field of bat;:
(4th August 1265). As regards the personal character f
De Montfort, it is not surprising to find that contempori ; ■
opinion v/as divided ; bub of his determination, cons Lam ■ ,
and energy there can be no question, while much is ;■•
vealed by the fact that, though in an unauthorized v; ; .
his memory was revered in England as a saint and mart;, i
offices were dra^^Ti up in his honour, his intercession in-
voked, and miracidous virtues attributed to. his relics.
The painstaking labours of recent investigators have tended
to bring into clearerlight the purity and nobleness of pur-
pose of Simon do Montfort as a consistent defender of the
rights of the governed ; on the other hand, it has also be-
come ob%dou3 that the representative institutions of Eng-
land, though largely helped forward by him, can hardly be
claimed as his ci-eation. Thus on both sides the statement
of Hujno that the House of Commons was planted by tj'.f
inauspicious hand of this bold and artful conspirator must
be rejected as inconsistent with the facts.
Coraparo England, vol. viii. p. 310 sqg., and see the monoj^i-aphs
of Paiili {SL?non von Montfort^ Oraf von, Leicester^ Dcr Schi}tfcr ar«-
Hauscs dcr Ocmeiucn, Tubingen, 1867) and Protliero (Tlie Life of
Simon de Montfort, 1877), and the literatin-e tlieio referred to.
MONTGOMERY (Welsh, Sivj/dd Tre Faldiv7jn\ an
inland comity of Wales, is boimded E. by Shropshire, N.E.
by Denbigh, N.W. by Jlerioneth, S.W. by Cardigan, and S.
by Radnor.. Its greatest length from soutli-east to north-
west is about 40 miles, and its breadth from east to west
about .35 miles. The area is 495,089 acres, or about 773
square miles. The surface is broken and undulating,
but it is only round the borders of the county that the
hills rea,ch any great height, the highest summits of the
diflferent ranges being generally in the adjoining countit
To the north are the Berwyn chain, stretching into Denbi;:! :
shire, in the east the Breidden hiiU, in the soutli the Ker. ,
hills, and in the south-west Plinlimmon, the hi'^iiest stmimii
of which is in Cardigan. These various mountain range,
form the watershed of the numerous rivers of jUontgomer\
shire. With the exception of the Dyfi, which rises nc?,.
Bala Lake and falls into Cardigan Bay, and the Wye, whic!:
flows south into Radnorshire, all the principal rivers r.r^
, tributaries of the Severn (Welsh, Hafrcn), which rises on
the east side of Plinhmmon and traverses the whole length
of the county from south-west to north-east. The principal
of these tributaries are the Clyvvetlog, the Taranon, t;. .
Rhiew, and the Vyrnwy. This fine succession of ri'vi r
valleys broaden out as they reach the great vale of th
Severn, and the beauty of the scenery is enhanced by :.:
abundance of oak and other trees. The Mcntgomcryshh^
canal, which has a length of 27 miles, and passes the
principal towiie, is connected with the EUesmere canal,
thus affording water commtinication mth Chester and
Shrewsbury.
Montgomcry-shire is occupied chiefly by Lower Silurir ■ :
rocks. Tlio boundary between it and Merioneth is forny !
by the Bala beds. In the centre and cast, near Llani'.i r
and Slontgomery, Wenlock shales i^rcvail. In the nri);i
bourhood of Welshpool the Silurian rocks jiave been fr^
qucntlv dLilocated by volcanic masses, one of the mcit
M O N — M O N
789
remarkable of which is Corndon Hill, rising to a height of
1700 feet. In some places the sedimentary rocks have
been penetrated by trap mingled with shale or schist.
Along the lines of dislocation there are frequent deposits
of metallic lodes, carried there by the heated water rising
from below. The lead mines of Montgomeryshire are of con-
siderable importance, and at present the metal is wrought
at seven different places. In 1881 the amount of lead ore
obtained in the various mines was 3432 tons, yielding 2693
toas of lead and 25,432 oz. of silver, the total value being
.£30,495. There were also obtained 1414 tons of zinc
ore, yielding 610 tons of zinc, of a total value of £3231.
Agriculture. — The climate is mild and genial, and the soil in the
valleys remarkably fertile, especially along the banks of the Severn.
A considerable portion on the borders of Merioneth is, however,
oocnpied chiefly by heath and moss. The number of holdings has
been rather decreasing of late years, the decrease being chiefly in
those below 50 acres in extent, which in 1880 (the latest year
regarding which there is information) numbered 3572, while there
■were 1650 between 50 and 300 acres, and 45 above 300 acres, of
which 2 were above 1000. According to tlio agricultural returns of
1382, the total area of arable land was 266,084 acres, or nearly one-
ti.ilf of the whole. Of this 63,538 were under com crops, 163,441
•were permanent pasture, 23,882 rotation gi'asses, and only 11,107
green crops ; 457 acre.5 were under orchards, 2 under market gardens,
37 under nursery grounds, and 22,744 under wooib. Of the corn
crops, wheat occupied 18,665 acres, and oats 23,937 acres. Cattle,
wliich are chie.ly Hereforda and cross-breeds, tliongh there are some
Devons and a few of the old Montgomeryshire breed, numbered
02,033 in 1832, of which 21,912 were cows and heifers in milk or in
calf. Horses in 1882 numbered 13,985, of which 7060 were used
solely for agricultural purposes. Tlio county was long famous for
ita liardy breed of small horsed called merlins, which are still to be
met with. JIany good hunter.'i and cart-horses are now bred. The
number of sheep in 1882 was 305,641. On some of the heath lands
in the centre and west of the county a diminutive breed of sheep
c.iUcd c'.uns is pastured, but those kept in the better cultivated
regions are principally Shropsliiro Downs. According to the latest
Toturn, tbo land was divided am.ong 3241 proprietors, possessing
3S7,S42 acres, with a gloss annual rental of £378,612. Of these,
1314, or 40 j)cr cent., possessed less than one acre, 32 possessed
: uTWCcn 1000 and 2000 acres, and 25 between 2000 and 5000 ; the
following possessed upwards of 5000 acres, viz. — Earl Powis, 33,645 ;
Sir \V. W. Wynn, 32,963 ; Lord Sudcley, 17,168 ; J. Naylor, 9276 ;
and marquis of Londonderry, 7400.
Manvfaclures. — In all the towns the manufachire of woollen
cloth, especially Welsh flannel, is earned on, ,and althongh the
industry was lately on the decline it is now reviving.
Administralimi and Population. ~~yio\itgo\mry^nT& comprises
nice hundreds, and the municipal boroughs of Llanidloes (3421) and
Welshpool (7107). Llanfyllin, Uanidloes, Machynlleth, Mont-
gomery, Newtown, and Welshpool form the Montgomery district of
borough?, with a total population in 1881 of 19,925, and return one
member to parliament. One member is also returned for the county.
Moutgomcryeliire is p.iitly in the dioceses of Bangor, Hereford, and
St Asaph, and contains sucty-eight civil parishes, townships, or
places, as well as parts of other parishes in .adioining counties. From
65,7G0 in 1601 the population had increased in 1851 to 67,33.'i, and
mVn to 67,623, but in 1881 ithad duniuishod to 65,718, of whom
33,004 were m.iles and 32,714 females.
ffiit^nt. — At the time of the Roman invasion, Montgomery was
possessed by a tribe of the CjTnri called Ordovices. Traces of
several of tlio old British camps still remain, the principal being
those at Dolarddyn, on Breidden Hill, and at Caereinion. There are
also a large number of cairas and barrows. The county was tra-
versed by the great Roman road, the J'ia Dcvana, which was joined
Ijy .■•. number of others ; but the remains of Roman camps or stations
am unimportant. .After being vacated by the Romans, little is
known of the history of Montgomery, until Wales was subdivided
into three districts at the death of Rhodii the Great. Montgomery
was then included under Powj-s, and formed the chief portion of
Powya Gwcnwynwyn, sometimes called Upper Powys. Powys or
Pov.T.! f.istle, the seat of tho nilcrs of Upper Powys, was founded in
1103. Ealdwyn, from which the county takes its Welsh name, was
lieutenont of tho marches ; and, for the purpose of holding the dis-
trict in check, a cistle was built about the e«d of the lltli centuiy,
which, after being captured by the natives, was retaken by Roger
<lo iiontgomcry. He gave his name to tho castle, and to tho sur-
tfDunding district of ancient Powyg, which was made a couuty by
Henry VIIL in 1533.
MojrTGOMERY, the county town, is situated on the decli-
vity of a well-wooded hi!! near tlie eastern bank of the
Severn. 21^ miles south by vast of Shrewsb'iry, and IST'J
by rail ncrth-'.rest by north of London. It is a clean and
well-built tov/n, but somewhat scattered and irregular.
The principal building.^ are the parish church of Saint
Nicholas (an old cruciforju structure) and tlie town-haU.
The borough has returned members to parliament since
the time of Heniy Arm., but by the Reform Act of 1832 it
was constituted one of the Montgoraeiy district of boroughs,
which together return one member. The population of
the borough (area, 3323 acres) was 1194 in 1881.
There are only a few crumbling remains of the old fortress of
Montgomery, originally founded in tlie time of William the Con-
queror to overawe the Welsh, and held by Roger de Montgomery,
from whom the town takes its name. The castle was greatly
enlarged in tho time of Henry IIL, when it was the scene of fre-
quent contests between that monarch and Llewelyn the Great. In
the 14 th century it was held by the Jlortimers, from whom it passed
to tho house of York. By the crown it was granted in the IStli
centiu-y to the Herberts of Cherbnry, but during the Civil War it
was surrendered by Lord Herbert of Cherburj- to the Parliamentary
forces, by whom it was dismantled.
MONTGOMERY, a district in the lieutenant-governor-
ship of the Punjab, lying between 29° 58' and 31° 33' N.
lat., and between 72° 29' and 74° 10' E. long., is bounded
on the N.E. by L^ihore, on the S.E. by the river Sutlej,
on the S.W. by Jlultjn, and on the N.W. by Jhang. The
area is 5573 square miles. Montgomery district, formerly
known as Gugaira, occupies a wide extent of the Biri
DoAb, or wedge of land betv/een the Sutlej and the E4vi,
besides stretching across tho latter river into the adjoining
Eechna Do4b. In the former tract a fringe of cultivated
lowland skirts the bank of either river, but the whole
interior upland c(»isists of a desert plateau partially over-
grown with brashwood and coarse grass, and in places witli
impenetrable jungle. On the farther side of the Rivi,
again, the country at once assumes the same desert aspect.
The census of 1863 returned the population at 359,437 (males
200,016, females 159,421), viz., Hindus, 69,805; Mohammedans,
277,291 ; Sikhs, 12,286 ; and "others," 55. The J.its, or pastoral
tribe, form the most distinctive class i.i the district. They bear
the name of " Great Ravi," in contradistinction to the purely agri-
CTiltural classes, who are contemptuously styled "Little Rivi."
They possesses fine physique, with handsome features, claim a
Rajput ancestry, and despise all who handle the plough. In
former days they exercised practical sovereignty over the agricul-
tural tribes. Only two towns in the district contain over 5000
inhabitants, viz., Pak Pattan (6086) and Kamalia (5695). The
town of Montgomery, the headquarters station, had a population of
onlv 2116 in 1SG8.
Out of a total assessed ares of 3,569,746 acres, only 538,240 aie
retuined as under cultivation. In 1872-73 the rail (or spring
harvest) acreoge was as follows :— wheat (the chief crop), 162,989
acres; barley, 30,134; gram, 21,416; mustard, 2077 ; and tobacco,
1303 acres. In the same year the kharif{ox autumn harvest) acreage
was:— j/'oiir, 20,509 acres; rice, 18,727; cotton, 16,916; (li, 12,46?;
kayfgni, 9493 ; and sugar-cane, 493 acres. Irrigation is practisetl
from rivers, canals, and wells ; the tot.al area ii'iigatcd by pnblic
works is 66,495 acres, and by private works, 158,709. Tlte desert
uplands afi'ord after the rains a scanty pasturage for the scattered
herds of tho Great Ravi Jdts, and yield an impure carbonate of soda
[sajji) from the alkaline pl.-mts with which they abound. The com-
mercial staples include wheat, rice, gi'am, millets, cotton, woo), aAi",
hides, and sajji. Large numbers of camels are bred for exportation.
The imports comprise sugar, salt, oil, English piece goods, metals,
indigo, and fruits. The manufactures consist of country cloth,
coai-se striped silk, and lacquered wood-work. The Lahore and
Mi'dtan railway intersects the district, which is also traversed in
every direction by good unmctalled highways. The revenue of the
district in 1871-72 amounted to £47,954, of which £42,355 was
derived from the land-tax. Education in 1871-72 was afforded by
59 aided and unaided schools, with a total of 1417 ])upils. The
average annual rainfall for tho seven years ending 16/2-73 was 9 '6
inches.
From time immemorial the Rechna Dcib has formed the home
of a wild race of pastoral Jats, who have constantly maintained a
sturdy independence against the successive rulers of northern India.
The historians of Alexander's invasion mention a tribe called tho
Cathseans, who probably had their capital at Sangala in the Jhang
district, and the ilalli with their metropolis at Miiltdn, as in
possession of this part of the counti-y. "Fne sites of Kot Kamalia
and Harappa in Montgomery contain large mounds of anti(^uo
bricks and other ruins, while many other r'.'inains of ancient cities
"90
M O N — ^I O N
or villages lie sc.ittorca along the river bnuk, or dot the now barren
stretches of the central wasto, clearly mr.rking the former ej-istonce
of a consiUerable nopiilatiou. The [i-iotoral tribes of this barren
expanse do not appear to have paid more than a nominal allegiance
to the Moslem rulers, and even in bfer days, when Ranji't Sinh
cxteuded the Sikh supremacy as far as Jli'dtau, the country yielded
little or no revenue, and the population for the most part re-
mained in a chronic state of rebellion. British influence was first
exorcised in the district in 1S47, when an oflicer was deputed to
cflect a summary settlement of the land revenue. Direct British
rule was effected on the annexation of the Punjab in 1849. The
only incident since then was a general rising of fho wild clans dur-
ing the mutiny of lSj7, several actions being fought before the
clans were defeated and dispcreed and order restored.
MOXTGOJEERY, a city of the United States, the
capital of Alabama, is built on a high bluff on the left
batik of the Alabama river, 158 miles north-east of Mobile,
with which it is connected by rail (180 miles) and by a
steamboat service (330 miles). The State-house, rebuilt
in 1851 at a cost of 875,000, occupies a commanding
aite on Capitol Hill. There are a city-hall, a court-house,
and two theatres, a large flour-mill, a cotton-factory, two
oil-mills, a fertilizer-factory, and seTeral foimdries and
machine shops. The population was 16,713 in 1880; and,
ill consequence of the marked increase in commercial and
industrial activity since that date, it is now (1883) esti-
mated at 19,000. Founded in 1817, and named after
General Richard Montgomery (173G-75), the town of Jlout-
gomery became in 1847 tha seat of the State Gove nment
instead of Tuscaloosa. From February 1861 to May 18G2
it was the capital of the Southern Confederation. In 1S65
it was seized by the Federal forces under General ^Tilson.
MONTGOMERY, Alexandee, whoso life fell between
1550 and 1610, was the last of the series of Scottish poets
who flourished in the 16th century under the patronage of
the Jameses. With the union of the crowns, and the
transference of James ^^. from Edinburgh to London,
court favour was withdra^vn from Lowland Scotch ; it
practically ceased to be a literary language, and no poetry
of mark was written in the dialect, if we except that of
Allan Ramsay's school, tUl it reappeared in literature as
the instrument of the Ayrshire peasant. By a curious
coincidence, Montgomery seems to have been, like Burns, a
native of Ayrshire. A commendatory sonnet from his
pen, extravagantly nattermg, as was the custom of the
time, was printed with ICing James's Essays of a rnnUce
in 1584 ; he received a pension from the crown a few
years later, fell into disgrace apparently for a time, ■was
reinstated in favour, and accompanied his patron to Eng-
land. As might be cxi^ectfd from the poet of a coiirt
where the king himself was a keen critic, Jlontgomery's
miscellaneous poems show a carefid attention to form ; he
tried many metrical experiments, and managed many
complicated staves with skill. The sonnet form, .at that
tln-.e a leading fashion in English verse, was also cultivated
at the Scottish court, and Jlontgomery's sonnets possess
conisidorable merit. His most successful poem, published
in 1597, and frequently reprinted in Scotland, was the
ullcgoiT of The Cherry and the Slae. The poet, smitten
by Cupid, conceives a longing for some cherries, beautiful
fruit, but growing high up on a steep and dangerous bank,
fibove a roaring waterfall. Shall he climb and win ?
Hope and courage and will urge him to try ; dread and
danger and despair counsel him to bo content with the
humbler fruit of the sloe, which grows within easy reach.
Experience, reason, wit, and slcill debate the question.
In the end he resolves to venture for the cherry, with the i
active help of these last-named powers. The conflicting
counsels of the poet's advisers are very pithily expressed in
proverbs for and against the adventurous enterprise, and the
description of the situation is strong and vivid. Mont-
gomery was no unworthy successor to Henryson and
Dunbar in executive finish, but the want of originality in
his poems shows that the old impulse was nearly ex-
hausted. There are traces of Italian influence in his
sonnets and love songs, but it was much less powerful
with him than ^vith his English contemporaries.
MONTGOMERY, James (1771-1854), poet and jour-
nalist, was justly described by Lord Byron, in a footnote
to English Bards and Scotch Revifwers, as "a man of con-
siderable genius," though it was going far beyond the mark
to speak of his Wanderer of Svjilzerkcnd (his first notable
poem, published in 180G) as being worth a thouscnd
" Lyrical Ballads." Montgomery was born 4th Xovtm-
ber 1771, at Irvine in Ayrshire, Scotland. Part of his boy-
hood was spent in Ireland, but ho received his education
in Yorkshire, at the Moravian school of Fulneck, named
after the original home of the iloravians, to which sect his
father belonged. He drifted at an early age into journaUsm,
and edited the Sheffield Iris for more than thirty years.
When he began his career the position of a Dissenting jour-
n-aUst was a difficult one, and he twice suffered imprisonment
(in 1795 and 1796)on charges that now seemabsurdlyforced
and unfair. His Wanderer was mercilessly ridiculed by the
Edinburgh Review, but in spite of this Montgomery pub-
lished many poems, which had a wide popularity ; — The
West Indies, 1810; The World Before the Flood, 1812;
Greenland, 1819; Songs ofZion, 1822 ; Tlie Pelican Island,
1827. On account of the religious character of his poetry,
he is sometimes confounded with Pu)bcrt Montgomery, very
much to the injustice of his reputation The inspiring force
of James Montgomery's poetry was the humanitarian senti-
ment which has been such a power in the political chan;jc3
of this century, and the pulse of this sentiment is nowhcro
felt beating more strongly than in his verse. His poe'.:-y
has thus an historical interest altogether apart froni irs
intrinsic value as poetry. But this value is far from ct ii-
temptible or commonplace. Stiictly speaking, Montgomc ; y
was more of a rhetorician than a poet, but his imaginati' a
was bold, ardent, and fertile, and more than one of his greater
contemporaries owed occasional debts to his vigorous inven-
tion and even to his casual felicities of diction, while soce
passages from his poems keep a place in the literature that
is imiversally read and'quoted. ■ At the close of his cai'err
as a journalist, when all parties agreed in pajnng him
respect, he claimed for his poetry that it was at len.st not
imitative, and the claim was just as regarded conception
and choice of subjects; but as regards diction and imagery
the influence of Campbell is very apparent in his earliev
poems, and the influence of Shelley is supreme in tlie
Pelican Island, liis last and best work as a poet. Bis
Lectures on, Poetry and General Literature, published in
1S33, show considerable breadth of sjnnpathy and power
of expression. Memoirs of him were published in seven
volumes in 1856-8. They furnish valuable materials for
the history of English provincial politics in the 19th
century. He died at Sheflield 30th April 1854.
MONTGOMERY, Robert (1 807-1855), author of The
Omnipresence of tlie Deity (1828), Satan (1830), and Tut
Messiah (1832), was the Montgomery ridiculed and de-
nounced in Macaulay's famous essay. As a poet, he deserved
every word of Macaulay's severe censure ; the marks of
intellectual feebleness — tautologous epithets, absurdly
mi^ed metaphors, and inapt lines introduced for the sake
of rhyme — are visible in every page of his versification.
It should bo mentioned that MacaiJay's " trouncing " did
not diminish the sale of his so-called poems ; one of the
works expressly ridiculed reached its 28th edition in IS5S.
His real name is said to have been Gomery.
MONTH. See Astronomy, vol. ii. p. 800, and
Cale-vdah.
MOXTILLA, a small and unimportant city of Spain in
M 0 N — M O N
791
fjie province of Cordova, 32 miles to the south of the city
of Cordova, on the Malaga railway, is strikiDgly situated on
two hills which command a bsautiful and extensive prospect
of the surrounding country. The manufactures (princi-
pally weaving) are xxnimportant, and the trade of the place
is chiefly in agricultural produce. The oil of the surround-
ing district is abundant and good ; and it is the peculiar
flavour of the pala dry light wine of Montilla that gives
its name to the sherry known as Amontillado. The popu"
ktion in 1878 was 13,207. McntiUa was the birthplace
Off " The Great Captain," and stiU shows the ruins of the
castle of his father, Don Pedro Fernandez de Cordova.
MONTLUG, BL.iisE de La3sekan-Massenc6me, Seiq-
NETTR DE (c. 1503-1577), marshal of France, was bom
about 1503, at the family seat near Condom in the
modern department of Gers. He was the eldest son, and
his family was a good one, but it was large and poor, and,
like most gentlemen of Oascony, he had to trust for endow-
ment to his sword. He served first as a private archer and
man-at-arms in Italy, with Bayard for his captain, fought
all through the wars of Francis I., and was knighted on
the field of C^risoles (1538). Having apparently enjoyed
no patronage, he was by this time a man of middle age.
Thenceforward, however, his merits were recognized by his
appointment to various important posts. His chief feat was
the famous defence of Siena (1555), which he has told so
ailmirably. When the religious wars broke out in France,
Moctluc, a staunch royalist, held Guienne for the king,
a:id exercised severe but impartial justice on Catholics and
Trotestants alike. He would have nothing to do with the
Massacre of St Bartholomew. Hem-y III., however, made
hiai marshal of France, an honour which he had earned by
nearly half a century of service and by numerous wounds.
He died at Estillac near Agen in 1 577. Montluc's eminence
above other soldiers of fortune in his day is due to his
Commentairea (Bordeaux, 1592), in which he described his
fifty years of ser\-ice. This book, the " soldier's Bible" (or
" breviary," according to others), as Henry IV. called it, is
one of the most admirable of the many admirable books of
memoirs produced by the unlearned gentry of France at that
time. It is said to have been dictated, which may possibly
account in some degree for the singular vivacity and
picturesqueness of the style. Hardly any author excels
Montluo in the clearness with which he brings military
ojicrations before the reader. As with most of his con-
temporaries, his work is didactic in purpose, and he often
pauses to draw morals for the benefit of young commanders,
but never tediously. The eloquence displayed in some of
the speeches is remarkable. These Commentaires are to be
found conveniently in the collection of Michaud and
Poujoulat, but the standard edition is that of the Societi
de VHistoire de France, edited by M. de Ruble (5 vols.
1865-72).
MOXTLUCON', the industrial capital of the centre of
Franco, sometimes called the French Manchester, is the
head of an arrondiisement, and the largest to^-n (26,079
inhabitants in 1881) of the department of Allier. The
upper town consists of steep, narrow, winding streets, and
preserves several buildings of the 15th and 16th centuries ;
the lower toi^Ti, traversed by the river Cher (there converted
into a canal communicating with that along the Loire), is
the seat of the manufacturing industries, which embrace
glass, steel, and n-on works, lime-kilns, saw-mills, and a
wool-spinning factory The Commentiy coal-mines are
ordy a few imles distant. There is railway connexion with
Mouliiis (50 miles to the east-north-east), Bourges, Limoges,
and Clermont-Ferrand, and a new Une ia about to be opened
to Tours via Chateaurou.x. Of the churches, Notre Dame
is of the 15th century, St Pierre partly of the 12th, and St
Paul modem. The town-hall, with a library, occupies the
sue of an old Ursuline convent, and two other con' ents now
serve as college and hospital.
Montlujon, wbiuli eiiisted as early as the 10th century, was taten
by the English in 1171 and by Philippe Auguste in 1181 ; the EngUsli
were beaten under its walls in the 1 4th century. The castlo, rebuilt
by Louis II., duke of Bourbon, was taken by Henry IV. during the
religious wars ; at present it is occupied as a barracks.
MONTMORENCY, the name of one of the oldest and
most distinguished families in France, is derived from
Montmorency, now in the department of Seine-et-Oise, Jn
the immediate neighbourhood of Enghien and St Denis,
and about 9 miles to the north-north-west of Paris. The
family, since its first appearance in history in the person of
BoxJCHAED or BcECH-iRD I., sire de Montmorency in the 10th
century, has furnished six constables and twelve marshals
of France, several admirals and cardinals, numerous grand
oflScers of the crown and gi-and masters of various knightly
orders, and was declared by Henry TV. to be, after that of
the Bourbons, the first house in Europe. Matthieu I., sire
de Montmorency, received in 1 1 38 the post of constable, and
died in 1 1 60. • His first wife was Aline, the natural daughter
of Henry I. of England ; his second, Adelaide or Alice of
Savoy, widow of Louis VI. and mother of Louis VII.
According to Duchesne, he shared the regency of France
with Suger, during the absence of the latter king on the
second crusade. Matthieu II. had an important share
in the victory of Bouvines (1214), and was made grand
constable in 1218. Durioig the reign of Louis YIII.
(1223-1226) he distinguished himself chiefly in the south
of France (Niort, Rochelle, Bordeaux). On the accession
of Louis IX. he was one of the chief supports of the queen-
regent Blanche of Castile, and was successfid in reducing
all the vassals to obedience. He died in 1 230. His younger
son, Guy, in right of his mother, became head of the house of
Montmorency-Laval. Anne do Montmorency (1-193-1567),
so named, it is said, after his godmother Anne of Brittany,
was the first to attain the ducal title. He was bom at
Chantilly in 1493, and was brought up with the dauphin,
afterwards Francis I., whom he followed into Italy in 1515,
distinguishing himself especially at Mariguano. In 1516
he became governor of Novara ; in 1520 he was present at
the Field of Cloth of Gold, and afterwards had charge of
important negotiations in England. Successful in the
defence of Meziferes (1521), and as commander of the Swiss
troops in the ItaHaa campaign of the same year, he was
made marshal of France in 1522, accompanied Francis into
Italy in 1524, and was taken prisoner at Pavia in 1525,
Released soon afterwards, he was one of the negotiators of
the treaty of Madrid, and in 1530 reconducted the king's
sons into France. On the renewal of the war by Charles
V.'s invasion of France in 1536, Montmorency compelled
the emperor to raise the siege of Marseilles ; he afterwards
accompanied the king of France into Picardy, and on the
termination of the Netherlands campaign marched to the
relief of Turin. In 1538, on the ratification of the ten
years' truce, he was rewarded with the office of constable,
but in 1511 he fell into disgrace, and did not return to
public life until the accession of Henry II. in 1547. In
1548 he repressed the insurrections in the south-west,
particularly at Bordeaux, with great severity, and in 1549-
1550 conducted the war in the Boulonnais, negotiating the
treaty for the surrender of Boulogne on 24th March 1550;
In 1551 his barony was erected into a duchy. Soon after-
wards his armies found emplojnaent in the north-east in
connexion with the seizure of Metz, Tou), and Verdiuj by
the French king. His attempt to relieve St Quentin issued
in his defeat and captivity (10th August 1557), and he did
not regain his liberty until the peace of Cateau-Cambr^sis
in 1559. Supplanted in the interval by the Guises, he yn.i
treated with coldness by the new king, Francis II., and
compelled to give up bis mastership of the royal house-
792
MO N — Ai O N
liold, — hia son, however, being appointed ma^^■.]lal by vr,\y
of indemnity. On the accession of Charles IX. in K'GO
he resumed his offices and dignities, and, uniting with hh
former enemies, tlie Guises, played an important port in t!:e
Huguenot war of 1562. Though the arms of hia party
were victorious at Dreux, he himself fell into the hands
of the enemy, and was not liberated until the treaty of
Amboise (19th March 1563). In 1567 he again triumpbrd
at St Denis, but received the death-bfow of which he died
3oon afterwards at Paris. His eldest son, FRAJi90isE do
Montmorency (1530-1579), was married to Diana, natural
daughter of Henry 11. ; another son, Henp.i I. da Mont-
morency (153-1-1614), was constable of France from 1593.
Henky n. (1595-1632), son of duke Henry I., succeeded to
the title in 161-1, having previously been i-aised by Louis
Xin. to the office of grand admiral. In 1625 he defeated
the French Protestant fleet under Soubise, and seized the
iilatids of Rh6 and Oleron, but the jealousy of Bichelieu
deprived him of the means of following up these advantages.
In 1628-1629 he was allowed to command against the duke
of Eohan in Lauguedoc ; in .1630 he defeated the piedmon-
tese, and captured Prince Doria, at Avigliana, and took
Saluces. In the same year he was created marshal. In 1632
he joined the party of Gaston, duke of Orleans, and placed
himself at the head of the rebel army, which was defeated
by Mar.shal Schomberg at Castekiaudary (1st September
1632); severely wounded, he fell into the enemy's hands,
and, abandoned by Gaston, was executed as a traitor at
Toulouse on 30th October. The title passed to his sister
OnASLOTTE-MAKGtjEEirE, princess of Cond6.
MO>f TOKO, a town of Spain, in the province of Cordova,
27 miles to the north-north-east of that city, on the Madrid
"■nilway, stands on a rocky peninsula on the south bank of
he Guadalquivir, here crossed by a fine bridge of four arohes
dating from the 16th century. Its most conspicuous build-
ing is a hospital, said to bo one of the best in Andalucia.
The most important article of commerce is the oil of the
surrounding district. The population of tho ayuntaniiento
was 13,293 in 1878.
MONTPELIER, a town of the United States, the capital
of Vermont (since 1 805), and the county seat of Washington
county (since 1811), is situated in 41° 17' N. lat. and 72°
Sty W. long., on the Winooski or Onion river, which faUs
into Lake Champlain. It has a station on the Central
Vermont Raih-oad, and is the western terminus of the
Montpelier and Wells River and the Montpelier and White
River Railroads. The State-house, in the form of a Greek
cross with a dome and Doric portico, was erected at a cost
of §150,000, to replace the structure burned down in 1857.
Under the portico stands a marble statue (by Larkin G.
Mead) of Ethan Allen (1737-1789), tho hero "of Vermont,
Tho State library contains 20,000 volumes. From 2411
in 1860 tho population had increased to 3219 in 1880.
JIONTPELLIER, chief town of the department of
Hijrault, Franco, is situated at the junction of several
railway lines, on a small hill rising above the Lez, at its
confluence mih the Merdanson, about 480 miles south of
Paris, and about 7 miles from tho McditeiTanean, from
which it is sejiaratcd by tho lagoons of Pfirols and I'Aruel.
As the headquarters of tho 16th corps d'armuo, as the seat
of a bishop, of a university, and of a court of appeal,
Montpellier is tho principal place of lower Lauguedoc. Tlie
Place du Peyrou, 575 feet in length by 410 in breadth,
one of the finest squai'cs in Franco, occupies the highest
part cf the town, and terminates in a terrace, commanding
a magnificent view of tho coasts of tho Mediterranean, and
of a wide stretch of country reaching to the Cevenncs on
'tho north, to the spiirs of t!;a Pyrenees on tho south-west,
and to those of the Alps on tlio north-cast. On the terrace
is situated the reservoir of tho tov;'n, the water being
brou:;ht from a d;-.t'''ncj of 5 ov 6 niil-;'! by an aqijeduct
of two tiers of arch.s, a'oout 70 icct in height. In the
centre cf the square is an equestrian statue of Louis XTV.
To the right and left aro promenades, on which the chief
boulevards converge. The Boulevard Ilenri FV. to the
north leads to the botanical garden, medical follege, and
cathedral ; to the east the Rue Nationale leads to the
palace of justice, the prefecture, and the citadel The cathe-
dral, which imtil 1536 Svas the church of .a Benedictine
monastei-y, suffered severely during the religious wars, but
about thirty years ago it was restored in the style of tho
13th century. It has four towers, and is one of the largest
churches in southern France, being more than 300 feet in
length, 92 in breadth, and 88 in height. The monastery,
after being converted into the bishop's palace, has since
1795 bemg occupied by the famous medical school. The
portrait of Rabelais hangs in the gallery of former profe,-:sors.
Connected vath the medical school is an anatomical museum
and a rich library. Montpellier also possesses a faculty
of science, with several fins collections, a faculty of letters,
a higher school of pharmacy, an agricultural college, and
a sericultural institute. The museum contains more than
600 paintings, in addition to collections of marbles, bronzes,
and antiquities. The botanical garden, more than 10 acres
in extent, is the oldest in France, having been laid out
in 1593. The esplanade, ornamented by fine old trees
planted by the due de Roquelaure, fomicrly governor
of Languedoc, leads towards the citadel. Tlie inner city has
nan-ow and tortuous streets, but many good houses. Among
the pnbHc buildings, the principal are the p.ila-co of justice
— a modern structure, the fa(;ade adorned %i ith statues of
the statesman Cambacer^s and of Cardinal Fleury— the
barracks, several hospitals, the juvenile seminary, and the
central prison for females. There are several ler.raed
societies, including an academy of Science and letters, an
antiquarian society, several medical societies, and others
for various separate branches of study, including the
dialect of Languedoc. The Lez has been deepened and
widened so as to connect Montpellier with the Canal du
Midi and with the sea at Palavas. The town has
a considerable trade in wine and brandy. The principal
industrial estabhshment is a manufactory for wax-tapers,
candles, and soap, doing business to the amount of X400,000
per annum. There are also chemical works, cooperages,
distilleries, &c. The population-in 1881 was 56,005.
Jlontpellier first rose Into importance after the destruction of
M.iguelone by Charles llartel in 737. Its prosperity dates fiom
tlie beginning of the ]2th centiu-y, -when ils tcliool of medicine
(see vol. XV. p. S07) first began to acquire fame. It lifld a school
of law in 1160, and a university was founded by Pope Nicholas IV.
in 1292. St Louis (Louis IX.) granted to the town the right of
free trade with the whole of tho kingdom, a privilege which greatly
increased its prosperity, in 1201 llontpeUier became a depend-oncy
of tliQ house of Aragon, through raarriaj^o, and in 1350-it was sold
to Philip of Valois. In the time of Charles VIII. it is said to have
had 35,000 hearths. It took tho place of the bishopric of Jlague-
loue in 1536. At tho time of th.. Reformation it became one of
the most important centres of Protestantism, but was taken by
Louis XIII., who erected tho citadel commanding the towTi.
Several years afterwards Jlontpellier was partly depopulated by
tho plaguo. Of the old fortifieations little now remains save the
gate of Peyrou, a triumphal arch of date 1712, ojuposita the place
of tlie same name.
Set? Gt-rmnin, Hisl-'ire du cmnmerce d« MontpfV.icr anflHfur.-mtnt i Toupfrivre
rfu part rfs Ct'.le p vols., 1801), and Htstoin 'tela <xmm\ir.c dc ilontpcllicrlSm^a.,
1651) ; Aisrcfouille, JlUU/iro de la villi dt ilonti,:!Uer (ISTV).
MO>rTPENSIER, Anne MAitra Louise d'OelSams,
DuciressE DE (162'7-1693), one of the most remarkable
names ou the somewhat arbitrary list of royal and noble
authors, was born at the Louvrel on 29th May 1627. Her
father was Gaston of Orleans, "Monsieur," tho brother of
Louis XIII., celebrated for the jnvaiiable ill fate which
attended his favourites and partisans. Her mother was
Marie de Bourbon, hoiv,--^ r-f tho Montpensicr family. Being
M 0 N — xM O N
793
thus of tlie .blood-royal of I'rance on both sides, and an
heiress to immense property, she appeared to be very c^.rly
destined to a splendid marriage. It was perhaps the greatest
misfortune of her life that " Slademoiselle " (as her courtesy
title went) was encouraged or thought herself encouraged
to look forward to the tlirone of France as t'la result of a
aiarriage with Louis XIV., who was, however, eleven years
hor junior. Ill-luck, or her own wilfulness, frustrated
numerous plans for marrying her to various persons of more
or less exalted station, including Charles II. of England,
tlisn Prince of Wales. She was just of age when the Fronde
broke out, and, attributing as she did her disappointments
to Mazarin, she sympathized with it not a little. It was
not, however, till the new or second Fronde that she dis-
i>!a,yed in a very curious fashion a temper and courage as
raasculine and adventurous as those of her father Gaston
h:\d alv.'ay3 been effeminate and timid. She not only took
r.'j.iiinal command of one of the aimies on the princes'
.'iUo, but she literally and in her own person took Orleans
by escalade, crossing the river, breaking a gate, and mount-
ing the walls with the applause of the populace of the city,
but in face of the refusal of the authorities to admit her.
Ko good result, however, came to her party from this
extraordinary act, and she had to retreat to Paris, where
■ she practically commanded the Bastille and the adjoining
part of the walls. On the 2d of July (16.52) tho battle
of iho Faubourg Saint Antoine, between the Frondeurs
under CondiS and the royal troops under Turenne, took
place, and the former, being beaten, found themselves in
an awkward situation, between their conquerors and the
walls of a city, which, though not exactly hostile to them,
was not nomiually on their side, and had closed its gates
against them. Mademoiselle saved them by giving orders
not merely for the gatos under her control to be opened
but for the cannon of the Bastille to fire on tho royalists,
v/liich was done. Her o_wn residence (and indeed her pro-
))t;rty) was the Luxembourg, and hero she found herself
<luring the riots which follo^^■ed the battle ; but in the
heat of the cmeute she installed herself in the hotel de
villc, and pla} ed the part of mediatrix between the opposed
parties. Her political importance lasted exactly six months,
ind did her little good, for it created a lifelong prejudice
agninst her in the mind of her cousin, Louis XIV., who
never forgave opposition to his sovereign power. Nor
h.id she any support to look for from her pusillanimous
father, who hastened to make terras for himself, — a matter
tlie less difficult that his known faithlessness had pre-
vented tho chiefs of the Fronde from engaging him at
all deeply in their schemes. Mademoiselle, on the other
hand, was for some years in disgrace, and resided on her
estates. It was not tiU 1657 that she reappeared at
court, but, though projects for marrying her were once
more set on foot, she was now past her first youth. Her
incurable self-will, moreover, still stood in licr way, and
suitor after suitor was rejected for reasons good or bad.
She was nearly forty, and had already corresponded
seriously with Madame de Motteville on tho project of
o.st-ablishing a ladies' society " sans mariage et sans amour,"
when a young Gascon gentleman named Puyguilhera,
afterwards celebrated as M. de Lauzun, attracted her atten-
tion. It was some years before the affair came to a crisis,
but at-lxst, in 1670, Mademoiselle solemnly demanded the
king's perinis-sion to maiTy Lajiizun. Jladame de Sevigne's
letter on tliis occasion is one of .the most famous of her
c^lection. Louis, who liked Lauzun, and who had ocon
educated by JIazarin in the idea that Madtmoiseile ought
not to be allowed to carry her vast estates and royal blood
to any one who was himself of the blood-royal, or even to
any foreign prince, gave his consent, but it was not inmio-
diately acted on. The pride of the other members of the
royal family, and the '.snit,3 o; the king's brother, Monsieur,
who had, after the death of Henrietta of EngUnd, made
offers to his cousin, prevailed with Louis to rescind hia
permission. Not long afterwards Lauzun, for another
cause, was imprisoned in Pignerol, and it v^as years before
Mademoiselle was able to buy his release from tlie king by
settling no small portion of her estates on Louis's bastards.
The elderly lovers (for in 1681, when Lauzun was roieased,
he was nearly fifty, and Mailefnoiselle was fifty-four) were
then secretly married, if indeed they had not gone through
the ceremony ten years pre^dously. But Lauzun, a coarse
and brutal adventurer, tyrannized over his ■n-ife, and her
spirit, which was yet unbroken, at length got the better of her
passion. It is said that on one occasion he addressed her
thus, " Louise d'Orleans, tire-moi mes bottes," and that she
at once and finally separated from him. She lived, how-
ever, for some years after he had achieved his last adven-
ture (that of assisting the family of James IT. to escape
from England, and attempting to defend their cause in
Ireland), gave herself to reUgious duties, and finished her
Memoires, which eStend to within seven years of her death
(9th April 1693), and which she had begun when she was
in disgrace t'oirty years earUer. These Memoires (Amster-
dam, 1729) are of very considerable merit and interest,
though, or perhaps because, they are extremely egotistical
and often extremely desultory. Mademoiselle \\Tites with-
out art, but ^vith tho hereditary ability of her family, and
the strongly personal view which she takes of public events
is rather an advantage than a disadvantage. They are to
be found in the great collection of Jliohaud and Poujoulat,
and have been frequently edited apart. (o. SA.)
MONTREAL, the largest city in the Dominion of
Canada, its chief seat of commerce and principal port of
entry, is situated on an island of about 30 miles in length
and 7 in breadth, at the confluence of the rivers Ottawa
and St Lawrence, 45° 32' N. lat. and 73° 32' W. long.
It stands at the head of ocean navigation, 160 miles above
Quebec, and nearly 1000 miles (9S6) from the Atlantic
Ocean, and lies at the foot of the great chain of river,
lake, and canal navigation which extends westward through
the great lakes. Montreal is btult upon a series of terraces,
the former levels of the river or of a more ancient sea.
Behind those rises Mount Royal, a mass of trap-rock thro-mi
up through tho surrovmding limestone strata to a height of
700 feet above the level of tho river. From this rock the
city derives its name, though its original founder, Paul do
Chomedey, sire de Maisonneuve, in 1612, gave it the name
of Ville-Marie, when it was dedicated with religious enthu-
siasm, not as a centre of commercial enterprise, but as the
scat of a mission which aimed specially at the conversion ^f
tho native Indians. The modern city of Montreal occupies
an area of about eight square miles, — its principal streets
running parallel with the river. On the north side of the
Mountain the Trenton limestone approaches the surface,
and is there quarried for building puij.oses. Of this giey
limestone most of the public edifices and many of the better
class of private dwellings are built. But both brick and
Avood are largely used for workshops and private houses of
a humbler class. The western slope of the Moitntain is
occupied by the Cote des Neiges (Roman Catholic) ceme-
tery, and the Mount Royal (Protestant) cemetery. The
upper portion of the Mountain, emb-.acing an area of 430
acres, is now laid out as a public park, with fine drives
shaded by well-grown trees. From its coramandmg site,
and tho wido expanse of the valley of the St La^vrence,
the views on all sides are of great variety and beauty.
A well-cultivated and wooded country, watered by the
Ottawa and the St Lawrence, stretches away on either
hand, being bounded on the west by the lakes of St Louis
and the Two Mountains, and on tlie distant horizon by
794
oi engmec, j,g sUll 13 a tubular iron brid™ supnorted
abu STr" °' ^°''^— ^7. -^thlleTmiS
lenotr T1,P r,- 'f™'' .^"^ '"measuring 9184 feet in
nour at th-> poin^jvL^.e it is tlius cros c1 and the
MONTREAL
I M GIU Coll „c
S. Uiristchurcn Cathedral (Ei.iocop )
5. Church of the Gesu ■"^•'i'.i
4. St Peter's CathedraL
6. Hallway Stition.
Plan 0' Jlonj-oal
6 Notre Dame.
7. Champ de Jlars.
8. Court House.
9. City Hall.
10. Bonsccours Market.
«rfr.= ! I A '°f 'P"''^- Near at hand the towers
spires, and domes of numerous churches and pubUc bifid
mgs r^se from the general mass of houses. ThethaTves"
ihlu . Lawence is navigable to Montreal bv
the largest ocean^ steamers. But immediately above thi
city the river 13 impeded by a natunl dvV^ V,f * !
limestone which he/e arrest^ the wa e at the . d'^ 'f
forming the Lake St Louis at a hei'ht of 44 0.?^'
the level of Montreal harbour. The rfver lIL f ■?
-y through a channel of .hoJtuTJul^l'Zl^
ft rajndity of about 18 miles an hour, formin- tl^^^tl V
or St Louis Rapids. O.-ing to the imme fse voE'of
vatcr concentrated in a narrow channel, steamerldrwin;
ten feet of water are safely navigated do^ the a Ms
but these necessarily present an insuperableTarrier to tt
Mrt of Ar ? ? ° ^''""^' '^'""''' ^°'"'»o.icing at the
^rt of Montreal, passes round the falls by a Series of
ocks in a course of nine miles, to Lalce St lii's, opposite
the Indian village of Caughnawaga. The fall of'^Cer
factories, estab!i;shcd on i-, \,'{.-. ^t • T^ °^^"
also been carried on heTe wUh'^ ^j profif "(vor^ '!?
cotton mills, silk factories a I->rle rabW f!,' f " ^'"^
cordage wo^ks, boot and' 'ho^ ^LSs t I™ '"T ""'^
organized on an extensive sea e tS t^l f"'^
Montreal is derived frorthrter Ibt^ T cKnd'
after passing along an open canal 5 miles in Tet'th It
posmg character ol mJjTth^l b^UiZ'^'ll!' m"^"'",-'""^
Ihedra of St Peter Aei{J.,.\ Vl "■"W"'*?^- The Metropohtan
0 chief featurefof St P^S^s at rZ™''"" °"-" ''l''"'^^^ ^"^l*
raiih church of Notro-Damp r.r, tl,„ m j,. "'J- ■''"'
oon^odation for 10.000 wo^s^ip^perf ^L^^Jellt? Ch„'"'r'-°
native limestone, but w?tWhe .iTiff ft'- '" t^'""?">' °^ ""^
modefof th;Om.»„ m ° memory a memorial cross, after the
ant denomiratiot tncluda St Gcor^.e'^';' r ' "t'" ^"'-'-
andSt Paul's fPresbvterianl Sf i ^ i/''S'i''='"' ^' --Andrew's
tie Pencfcan diantp:k?io7''¥l '"'V"™'','"^ children "f
s^iSti^^pSz-ii^SI^^-^i^^^t^:
PrenchlangiiaVs andiiterarif,,°!^'P"I'';^ '? *■>= English and
« ?epre"?nts T et T"' ^^ *° *°^^ "^ ^^' natio^.l ti ,vhi '
Ca. h^o 1™, lyla™ s/slr^^^ in Montreal, hut the^Kom^n
tlio a;,.L\^^ systematically discountenanced the eti.Te it,,!
Ksirar '■'* '■■*'"' -'■' >» "-» •■.. ..iss;
and accommodation is provided for the AdvV?,l V-i ^'""?^ '
striking to a atrrngor.^ ^""■'^•'^•^ """^ ^"''"J"^' f^" «»" i» very
M'Om Con' T'i-ljrl'''/;''"?'''''''''' '■"^tihi'i^s !a the nniversitv of
and ultimi ely became one of tlie leading merchants in Montreal
At his death in 1S13 ho left his iiroperty for the foundin" of a col-
lege, ihe most recent and liberal addition to it is the liter Re,l-
r,ath Jluseum, valued at upwards of SIOO.OOO, the gift of a wealthv
eitizen. 1 lie university embraces the faculties of arts, law anil
medicine, and has also a department of practical science. The
college buildings stand in a pleasant park fronting on Sherbrooko
otrcct, at the base of the Mountain. Theological collccs in con,
nection with the Church of England, the Presbyterian Methodisf*
ami ConOTcgational Churches, occupy buihliugs in the vicinitv, and
thoir students attend the claases at Jl'Gill College for secular instruc-
tion. The Seminary of St Sulpice is a theological training school
for priests, where the larger portion of the Roman Catholic cler^
of the province of Quebec have received their training, and also'ti
college where a large number of the French Canadian youth obtnin
their e<Iiication. This seminary is held in hii'h esteem, and attra.-ts
m-nny Koman Catholic students from the United States Laval
Lniv.r^uy, which has its chief seat at Quebec, has also a branch
at Mon re,-:l,_with a large staff of professors, chiefly in theolo-^-
hw, and mcaicine. The Jl'Gill and the Jacques Cartier Normal
Schools for ti-ainmg teachers for tno Protestant and Roman Catholic
rublio schools are conducted under the Protestant and Roman
Catholic boards of public instruction ; and model schools attached
to them afford the requisite practical training for teachers The
nrincinal public monuments are the column erected in honour of
Lord Nelson, and a bron/e statue of Queen Victoria, by the lato
Marshall A\ ooil, which occui.ics a good site in Victoria Square
ihe commerce of Jtontreal is well represented by the architec-
tural character of its banking establishments and many of the laree
mercantae houses. It is also tlie seat of a large manufacturing
industry. But the most substantial evidence of its importance al
a commercial centre is its harbour. The solidly-built basins
wharves, quays, and canal locks extend for upwards of a mile and
a half along the nver-side. In 18-19, at a period of depression, the
total value of the imports and exports amounted to £2,013 4?8
sterimg. In 1SS2 they had risen to £15,633,657 sterlins. The
business of the port at the same date is thus expressed in Canadian
currency:-totalvalueofoxportsS26,384,312,ofimport3S49,7J9 461-
customs duties collected estimated at 88,100,366. The number of
sca-gomg vessels in port was 648, of which fullv oue-half were ocean
steamers, lu addition to which the inland vessels ai'rivine at the
Fs°qfi? n« «n'' ^"t?" '^''° ,"«"'».'<=J ^•«''>« "( real estate in Montreal
IS 565 978,930. The population m 1851 numbered 57,715 ; in 1881
« 00. '"f?^«'l.t<'.lW,747 of whom 7S,CS4 were of French and
23,995 of Insh ongm, and of the whole number, 103,579 were Roman
Catholic.
The city returns three members to tho Canadian House of
Quew"^' ^""'^ number to the luovincial legislature of
When the first French explorers landed on the island of Montreal
under the leadcrsliip of Jacques Cartier in 1535, a laiOT Indian
palisaded town existed a little to the west of Jtount RoyaT, and not
far from the present English cathedral. To this fortified to«-n the
Indians gave the name of Hochelaga, and Jacques Cartier describes
it as surro-^nded by helds of giain and other evidences of a settled
native pcpnlation. The name is now applied to the eastern suburb
of the modern aty. Sixty years later, when Samuel de Cbamplain
Ztll'v ""J riP """ ^,' ^»"-^™«. "Od climbed to the sumnlit of
Mount Royal, the populous native town had disappeared, and onlv
two Indians wei-o found from whom some obscure hints were derived
of war between nv.-,l tribes, followed by the destruction of the town
and the extermination or (light of its former occupants. The enmitv
tnus established between the Wyandotts or Hurons of Canada and
tne Iroquois settled in th.e valley of the Hudson and south of Lake
Ontano was perpetuated throughout the whole period of French
occupation. Champlain took tho side of the Hurons while the
Iroc^ois allied themselves with the Dutch and English' settlers on
te Hudson. Thus the early histoiy of Montreal is largely occupied
^ith incidents of Indian warfare. In 1665 the marquis de Tracy
^^Idlei, «°?l ^!-'">"'.,l'""gi«g,."-itli him a regiment of French
soiclieis, with whose aid the Indian assailants were driven off, and
wt'.Tv .''",'^,S''"'''°'""J '0 '•'=P'=> 'heir incureions ; thus pro-
tected, Montreal became the centre of tho fur trade with the w'est
and en ered on its history as a commercial city. In 1722 it was
Dp Terv", .,"*, ^^•i°T',' ™" ^"'^ <'''<=''• ""'>" *1'8 directions of
Ti^n ^•' e '"° "S.''^' "'"^ "■'="='«'' on a '«='«''* now laid out »,
?f r^.Tw^iT""-,,-!?"' •"'''"" of 'i»'^"= ''y *''« English uude
MoXa- ^1„"'\^lT/'?"r'='* "" l°"g I'y'ho surrender of
Monti eau Since that date it has rapidly developed as an imnor
tant centre of commercial and manufactuHng enterprise! (D? W )
M O K — T^i O N
795
3I0NTE0SE, a royal and parliamentary borough and
teaport of Forfafshirc, Scotland, is situated on the German
Ocean at the mouth of the South Esk, on a branch of the
Caledonian EaUway, 30 miles east-north-east of Dundee
.-nd 36 south-south-Tvest of Aberdeen. Its harbour ba-in'
formed by the estuary of the South Esk, has an area of
about 4 square miles, and is dry at ebb-tide, but at hi"h
water there is a depth of about 18 feet at the bar. The
length of the quays and docks is about 1 \ miles. ' The
Soiith Eik IS crossed by a suspension bridge erected in
1S29 at a cost of £20,000, and having a length from the
points of suspension of 422 feet (with its approaches SOO
feet). On the links to the east of the town is one of the
finest golfing greens in Scotland. In the Ki-h Street
which is of considerable width, and contains several very
lofty houses, there are monuments to Sir Robert Peel and to
Joseph Hume, formerly member for the Montrose borou-hs
ihe principal buildings are the parish church— one of the
largest churches in Scotland— the town-house, tlie infirmanr
and the academy. There is a public library ^vith 19,000
volumes, and a mechanics' library with 7000 volumes
Besides the staple industry of flax-spinning, there arc
manufactures of linen, sail-cloth, sheetings, sfarcli, and
^"^P- Iro°-founding, tanning, and brewing are also carri=d
on. The e.xport trade is chiefly in manufactured goods
agricultural produce, and fish ; the principal imports are
timber and coal. In 18S1 the number of ships that
entered coastwise was 373 of 48,828 tons, tho number that
cleared 2o0 of 21,877 tons; the number engaged in the
n'o'S" ^"L'o'"""'' ^^^''^ '" *^'^ ^'-'""^ year was-entered
108 of 34,868 tons, cleared 42 of 10,359 tons. Montrose
is also one of the principal fishing-stations in Scotland the
number of registered boats in 1881 being 342 of 41GS
tons, giving constant employment to 697 persons, and occa-
sional employment to 300. Montrose joins with Arbroath
J3rechin, Forfar, and Inverbervie in returning one member
to parliament. The population of the royal bur'di in 1S71
was 15,720, and 16,280 in 1881 ; the population of the
parhamentary burgh in the same years was 14,452 and
14,975.
Montrose received a charter from David I. in the 12th ceiiturv
and was made a royal burgh by David II. in 1352. The town was
destroyed by fire m 1244. It was from the port of Montrose that
Sir James Douglas in 1330 embarked for the Holy Land witli the
heart of Bruce, and that Prince James Stuart, "the Old Preteiu er "^
The town is the birthplace of Andrew Melville, of the gi-cat marnu:s
of Montrose, and of Joseph Hume. !■ "I'qv-s
MONTROSE, James GRAH.iJi, Marquis of (161-'-
1650), born in 1612, became the fifth earl of Montrose by
his father's death in 1 626. He was educated at St Andrews ;
and in 1629, at the early age of seventeen, he married'
Magdalene Carnegie, daughter of the earl of Southesk. In
1636, on his way home from a prolonged visit to the Conti-
nent, he sought an introduction to Charles I., but, as it is said
was frustrated in his hope of obtaining the king's favour by
an intrigue of the marquis of Hamilton. Is'ot long after
the outbreak of the Scottish troubles in 1637 he'joined
the party of resistance, and was for some time its most
energetic champion. He had nothing puritanical iii his
nature, but he shared in the ill feeling aroused in tlie
Scottish nobility by the political authority given by
Charles to the bishops, and in the general indignation at
the king's ill-judged scheme of imposing upon Scotland a
liturgy which had been drawn up at the instigation of the
English court, and which had been corrected in England
by that Archbishop Laud who now became known in Scot-
land under the nickname of "the pope of Canterburj-."
Montrose's chivalrous enthusiasm eminently qualified him to
be the champion of a national cause, and the resistance if
Scotland was quite as much national as it was religio;-.^.
He signed the Covenant, and became one of the foremost.
Covenanters. The part assigned to him was the suppres-
sion of the opposition to the popular cause which arosu-
around Aberdeen and in the country of the Gordons. Three
times, in July 1638. ami in March and June 1639 Montrr .-tr
796
M 0 N — M 0 IS'
entered Aberdeen, where lie thoroughly succeeded in effect-
ing his object, on the second occasion carrying off the
licad of the Gordons, the marquis of Huntly, as a prisoner
to Edinburgh.
In July 1639, after the signature of the treaty of
Warwick, Montrose was one of the Covenanting leaders
■.vho visited Charles upon the borders. This change of
policy on his part is frequently ascribed to the fascination
of the king's conversation. In reality it arose from the
nature of his own convictions. He wished to get rid of
the bishops without making presbyters masters of the
.■>tata. His was essentially a layman's view of the situa-
tion. Taking no account of the real forces of the tirno,
lie aimed at an ideal form of society in which the clergy
should confine themselves to their spiritual duties, and in
V. Liich the king, after being enlightened by open communi-
<:'.tlon with the Scottish nation, should maintain law and
<;: dcrw-ithout respect of persons. In the Scottish parliament
wliich met in September, Montrose attempted to carry out
ihis policy, and found himself in opposition to Argyll, who
had placed himself at the head of the Presbyterian and
national party, which, by an alteration of the rules that
Iiad hitherto regulated the selection of the Lords of the
Articles, gave supremacy in parliament to the representa-
tives of the middle classes. Montrose, on the other hand,
wished to bring the king's authority to bear upon.parlia-
n;ent to defeat this object, and offered him the support of
a great number of the nobles, who were by this time as
much opposed to the predominance of the Presbyterian
clergy acting upon the middle classes as they had before
been opposed to the predominance of the bishops. He
failed, because Charles could not even then consent to
abandon the bishops, and because no Scottish party of any
■weight could be formed unless Presbytorianism were estab-
lished ecclesiastically.
llathcr than give way, Charles prepared in 1610 to in-
vade Scotland. As usual, he prepared difficulties for those
>vho wished to support him. Montrose was of necessity
driven to play something of a double part. In August
1340 he signed the Bond of Cumbernauld as a protest
against the particular and direct practising of a few — in
ot'ier \vords, against the ambition of Arg)-U. But ho took
his place amongst the defenders of his country, and in the
.•=amc month he Vv-as the first to wade across the Tweed at
the head of the invaders of England. After the invasion
liad been crowned with success, Montrose still continued
to cherish his now hopeless policy. On .'?7th Jlay 16-11
tie was summoned before the Committee of Estates charged
■with intrigues against Argyll, and on 11th June he was
imprisoned in Edinburgh Castle, ^^lien Charles visited
t^cotland to give his formal assent to the abolition of
Episcopacy, Montrose communicated to him his belief that
■flamilton was a traitor. It has indeed been alleged, on
•l.iarendon's authority, that he proposed to murder Hamilton
and ^Vi'gyll ; but this is in all probability only one of Claren-
don's miry blundei-s. His letters to Charles, however,
must be taken in connexion w ith this so-called incident.
During the progress of the investigation of this plot, Mon-
trose remained in custody, and upon the king's return to
England ho shared in the amnesty which was tacitlyaccorded
to all Charles's partisans.
Vor a time Slontrose retired, not voluntarily, from public
life. After the Civil War in England began he constantly
JM-Cised Charles to allow him to make a diversion on Scot-
land. At last in 164-1, ■when the Scottish army entered
England to take part against the king, Jlontrose, now
created a marquis, was allowed to try what he could do.
Ho set out lo invade Scotland with about 1000 men. But
Ills followers deserted, and his condition appeared hopc!cs«.
Genius, however, inspired him with courage. Disguised
as a groom, he, with only two gentlemen, started on IStli
August to make his way to the Highlands. No enterprise
might seem rasher. Highlanders had never before been
known to combine together, but 'Jloutrose knew that most
of the clans detested Argyll, not because they were royalist
but because Arg>-|l, as the head of the Campbells, was the
chief of an aggressive and unscrupulous tribe. Montrose
did not miscalculate his chances. The clans rallied to his
summons. About 2000 Irish had crossed the sea to assist
him. He won battle after battle. He defeated the Cove-
nanters at Tippermuir on 1st September, and at the Bridge
of Dee on 1 2th September. Rapidity of movement was tlie
•distinguisliing feature of his generalship. He crossed the
mountains deep with a winter's snow into the country of
Argyll, burning and destroying as ho rtsted for a time
from more active operations. On 2d February 1645 he
crushed the Campbells at Inverlochy, whilst the head of
the house, who was no warrior, looked on at the disaster
from a boat. The Scottish parliament declared Montros-i
to have forfeited his life and estate as a traitor, but it could
not reach bun to execute the sentence. On 19th February
he captured Elgin, tlirough March he was ravaging Aber-
deenshire and Kincardineshire, on 3d .April he stormed
Dundee, then on 9th ilay came the vlctorj' of Auldeain, on
2d July the victory of Alford, and on 1 5th August the great
victory of Kilsyth. Never till after this battle had Mon-
trose ventured far from the Highland hlUs. The High-
landers had the habit of running home after a victory to
secure their booty. Now, however, Montrose found himself
apparently master of Scotland. In the name of the king,
who now appointed him lord-lieutenant and captain-general
of Scotland, he sum.raoned a parliament to meet at Glasgow
on 20th October, In which he no doubt hoped to reconcile
loyal obedience to the king with the establishment of a
non-political Presbyterian clergy. That parliament never
met. In England Charles was in evil case. He had been
defeated at Naseby on 14th June, and Montrose must
come to his help if there was to be still a king to proclaim.
He never had a chance of knowing what Montrose could
do against the " new model " army David Leslie, the best
of the Scottish generals, was despatched against Montrose
to antlclpiate the invasion. On I'Jth September he came
upon Montrose, deserted by his H ighlanders and guarded
only by a little group of followeis, at Philiphaugh. He
won an easy victory. Montrose cut his way through to
the Highlands ; but he failed to reorganize an army. On
3d September 1646 he embarked fur Norway.
Montrose was to appear once mors on the stage of Scot-
tish history. In June 1649 he was restored by the exiled
Charles 11. to his nominal lieutenant-governorship of Scot-
land. In March 1600 he landed in the Orkneys to take
the command of a small force which ho had sent on before
him. Cro.sslng to the mainland, he tried to raise the clans,
but the clans would not rise, and on 27th April he vras
surprised and caiitured at Corblesdale in Ross-shire. On
ISth May ho entered Edinburgh as a prisoner. On the
20th he was sentenced to death by the parliament, and he
was hanged on the 21st, with AVishart's laudatory biography
of him put round his neck. To the last he protested that
he was a real Covenanter and a loyal subject. " The Cove-
nant which I took," ho said, " I own It and adiere to it.
Bishops, I care not for them ; I never Intended to advance
their interest." Something, at least, of Montrose's dream,
so impossible to realize at that time, has been realized in
Scotland. Scotland lias remained ecclesiastically Presby-
tcrlan. The political legality which Montrose wished to
upheld against factions by means of tlie Idng has been
upheld by means of th.a political ripeness of tho ScottUh
nation itself. (s. R. o.)
MONT ST MICHEL, a cuilous rocky islet, consisting
M O N — M O N
797
of A mass of granite about 3000 feet in ccrr.pass and 165
feet in height, rises at a distance of neoj-ly a mile from
the shore in the bay of St Michel, near the nouth of the
Cou&non, at the vertex of the angle formed by the coasts
of Brittany and Normandy. The quicksands by which it
is aarroiinded, and which stretch far to seaivard, ai e ex-
posed at low water, &nd highly dingcrou3 to those who
venture oa thcca Trithout a g-iide. Eecentlr efforts at
E8ckmatio!i have been made, and amongst other wo.'izs a
causeway has been constructed ccnn'.T.ting Mont St Michel
with the nearest point of the msinknd (near Moidrey) ;
an unfortunate consequence of these operations has been
that some portions of the ramparts of the island have been
gapped by_ the altered tidal currents. The fortress-abbey,
to which the rock owes its fame, stands upon the mere
precipitous sido towards the north and west ; the sloping
portion towards the east and south is occupied by dwelling-
houses. The strong machicolated and turreted wall- by
which tho whole is surrounded is pierced only by a single
gateway. The northward wall of the abbey (La Merveille),
dating from the 13th century, is of remarkable boldness;
it is 246 feet in length and 108 feet in height, is sup-
ported by twenty buttresses, and is pierced by a variety of
openings. The single street of the island, leading from
the one gateway up to the donjon of the fortress, is lined
with houses, most of them used as lodging-houses by
visitors and pilgrims ; it contains an old pamsh church,
and the house of Du Guesclin is also pointed out. The
abbey consists principally of two parallel buildings of
three stories each, that on the east containing hospitium,
refectory, and dormitory, and that on the west the cellar,
knights' hall, and cloister. The knights' hall is a superb
piece of Gothic architecture, measuring 85 feet by 59,
with three rows of richly-ornamented pillars. The cloister
is one of the purest and most graceful works of the 13th
century (1228). The church has a number of imperfect
tUiTets, and is surmounted by a square tower of the 17th
century, with a statue of St Michael, which was crowned
in 1877. The nave, which dates from the 11th century, is
Norman ; but the choir, which collapsed in 1421, has been
rebuilt in the flamboyant style. Beneath is a fine crypt.
Mont St Michel was ^ sacred place even in the time of the Druids.
It became a seat of Christian worship in the 8th century, when a
monastery was founded upon it (with the usual miraculous accom-
paniments) by St Aubei-t, bishop of Arranches. It soon became
3 favourite resort of pilgrims, not only from all parts of France, but
also from Great Brit^ and Ireland, and even from Italy. It was
plundered by the Normans ; but Rollo, on his conversion, made
restitution. At the time of the Conquest it supplied William of
Kormaudy with six ships, and received a considerable share of the
English spoils. " About this time the monks began to give them-
selves to learning and to collect a largo libraiy, and in the 12th
century the establishment reached its highest prosperity. It was
burnt by the troops of Philip Augustus, who afterwards fxu-nishcd
larce sums for its restoration (La ilen-eiUe). St Louis (Louis IX.)
made a pilgrima"e to Mont St llichcl, and was afterwards very liberal
to it During the hundred years' war it offered a memorable resist-
ance to the English ; and hero, on 1st August 14GS, Louis XI.
instituted the order of St Michel, and held a brilliant chapter. A
similar celebration was held by Francis I. Dining the religious
wars the Huguenots made repeated unsuci-essful attempts to seize
tlio fortress ; it opened its gates to Henry IV. after his abjuration.
About 1615 the Benedictine monks of Mont St >Iichel were re-
placed by monks of the Congregation of St JIaur ; after the Revolu-
tion tho abbey was used as a prison for political offenders. It is
now an histoncal monument; it contains an orphanage, and is under-
going repairs.
JIONTSERRAT, one ot the Leeward Islands in the
West Indie.?, situoted 16° 45' N. lat. and 62° 7' W. long.,
U 12 miles long and 8 broad in its widest part, and has an
area of 32 square niiies. The uneven and rugged surface
suggests possibly volcanic origin. Its general appearance
is very picturesque, the most interesting natural feature
being the Souffriere. The island was discovered by
Cdvunbus in 1493, and received its name either because
of its broken appearance or after the mountain in Spain.
It was colonized by the English under Sir Thomas Wamet
in 1632, and was taken by the French in 1664. Restored
to tho English in IOCS, it capitulated to the French in
1782, but was again restored in 1784. It is now a pre-
sidency under the general government at Antigua, and has
a legislative council, composed of oiBcjals and crown nomi-
nees. The cliTcate is tho most healthy in the West Indies.
Tiie population. (10,087) consists principally of negroes,
with several hundred whites. The revenue and expendi-
ture average .£5000 per.annum. Sugar exports range from
1200 to occasionally 2000 tons. An important industry
is the cultivation of limes and the manufacture of juice.
About 700 puncheons of raw lime juice, 300 hogsheads of
concentrated juice, and an increasing quantity of fresh green
limes are ezported annually. For the three years ending
18S0 the average value of imports was £26,390, of exports
£32,963. The principal town is Plymouth, lying midway
along the south-west coast.
MONTSERSAT. Thirty miles to the north-west of
Barcelona in Spain there rises a very remarkable mountain
of grey conglomerate, 24 miles in circumference, and at its
loftiest point (San Geronimo) a little more than 4000 feet
in height. From the comparative lowness of the surroimd-
ing district, and from its eitraordinaiy configuration, it is
a conspicuous object for many miles around. The mountain
consists of jagged pinnacles and spires rising abruptly from
the base of the mass, which is cloven with many clefts, and
abounds with steep precipices. It is the 2{cns Scrratvs of
the Romans, the Monte Serrado of the Spaniards, and is
thus named either in allusion to its jagged appearance, like
the teeth of a saw, or because the eastern face is split, as
if sawn, — which occurred, say the Spanish legends, at the
time of the crucifixion, when the rocks were rent. The
arms of the monastery represent a mountain with a saw
resting upon it and penetrating some distance into its mass.
Its pinnacles and pyramids apd sharp angular masses
resemble a mountain of hard crystalline volcanic tuff which
occurs between Akureyri and Kalmanstunga in Iceland.
The effect of Montserrat may be realized faintly if we place
oiu^elves upon the roof of Milan cathedral, and imagine the
forest of spires magnified a thousandfold. The central
spire will represent San Geronimo. Tlie result-of this varied
contour in the case of Montserrat is to make it one of the
most picturesque places in Europe. Paths wind along the
faces of the precipices, ascending to bare grey summits,
descending to sheltered valleys fiUed with evergreens and
flowers. The Pyrenees are seen in one direction, tho se.a in
another, while the Llobregat winds at the foot of the
mountain through the village of Monistrol. Manresa and
other villages are seen scattered over the plain ; and hills
covered with a warm red soil alternate with rich valleys.
Street says of Montserrat, — "Aftcj much experience of
mountains, it strikes ms more each time that I see it a£
among the very noblest of rocks."
The monastery, a great pile of buildings, stands upon a
narrow platform on the edge of a vast cliasra in the eastern
face of tho mountain. It owes its existence to an image
of the Virgin, said t® have been carved' by St Luke, and
brought to Barcelona by St Peter in 30 .t.D. When the
Moors invaded the province in 717, tho image was taken
to Montserrat and hidden in a cave. In 8 SO Gonderaar,
bishop of Vich, was attracted to the cava by sweet sounds
and smells, and there found the image, which he determined
to take to Manresa. But at a certain spot on the mountaii'.
the image refu.sed to proceed farther ; there it was consc-
ouently deposited, and a chapel was erected to contain it.
A stone cross near the walls' of the monastery still marks
the spot whore the imrxge refused to move. Round the
chapel a nunnery was built, and in 976 this was enlarged
798
M O N - - 31 0 O
and converted into a Benedictine monastery. Pliilip II.
liuilt the present church. In 1S35 the monastery was
suppressed and despoiled of the vast -treasured wki..h had
accumulated during the Middle Ages. But the buildings
were allowed to remain, as well as a few of the fathers to
take charge of the Virgin's shrine. At i)rcseut they number
19; a hundred years ago there were 76 monks, 28 lay-
brothers, 25 singing boys, together with surgeon, physician,
and servants. The possessions then consisted of numerous
hamlets, besides great quantities of plate and jewels, includ-
ing 85 silver lamps.
Nuestra SeSora de Slontserrat, Patrona de Cataluua, is ouo of the
■ most celebrated images in Spain, and her chuixh is visited annually
by more than 80,000 pilgrims. It is a small carved wooden image,
" regularly handsome, but the colour of a negro woman," and pos-
sesses magnificent robes and jewels. It has been visited by numbers
of sovereigns and high ecclesiastics, and by millions of Catalonians.
In September ISil it was solemnly crowned by Leo XIII., who sent
a crown from Rome for that purpose. Quantities of ex votos are
oficred at the shrine : wa.x models of injured or diseased limbs,
models of ships, pictures and clothes, jewels and silver hearts.
As the celebrity and sanctity of Montserrat increased, so did the
number of devotees. Ignatius Loyola laid his sword upon the- altar
of the Virgin, and, placing himself under her protection, started from
Montserrat to commence his new life. JIany eminent Spaniards,
weary of the w-orld, have retired to this monastery to end their days.
Some preferred solitary hermitages perched among the rocks. Of
these there w-ere fifteen, eleven of which onco formed a via sacra,
erding at the summit of San Geronimo. They were destroyed bv the
French, but the ruins of some of them still remain. From all the
vi:w is magnificent; some are indeed placed on the edges of preci-
jnces in almost inaccessible places. There arc also caves in the moun-
tain, some of which were formerly occupied by monks. The most
celebrated of these are the cave of the Virgin, in which the Santa
Ivicijcn remained hidden until found by Gondemar, and the cave
of I ray Juan tiarin, a notorious sinner, who ended his days in the
practice of revolting penances at Jloutserrat. At CoUbato, on the
south-east side of the mountain, near the base, there are also some
very curious caves.
MONTUCLA, JEAN-foiENNE (1725-1799), a learned
rattthematician, -was the .son of a merchant, and was born
at Lyons in 1725. He attended the college of the Jesuits
in his native city, and was early distinguished for his
t.iuacious memory and his aptitude for mathematics. At
the age of sixteen he removed to Toulouse to presecute the
study of law ; and after taking the asual degrees he re-
paired to Paris. There his conversational power.s, his solid
information, and his acquirements as a linguist soon intro-
duced him to the notice of. the learned. In the society of
D'Alembert and Lalande his taste for mathematical studies
was confirmed and stimulated. After publishing two anony-
mous treatises on the Quadrature of the Circle and on the
Duplication of the Cube, he gave to the world in 1758 the
first part of his great work, The Eistori/ of Mathematics.
>rot long after this his merits -(vere recognized by the
Government, and he was promoted to several important
offices. He was appointed intendant-secretary at Grenoble
in 1758, secretary to the expedition for colonizing Cayenne
in 176-1, and " premier commis des bailments " and censor-
royal foi; mathematical books in 1765. During the next
twenty-five years his time w-as divided between his official
duties and the study of his favourite science. The Revolu-
tion then ensuing deprived him of his income, and left him
in great destitution. The offer in 1795 of a mathematical
chair in one of the schools of Paris was declined on accoiuit
of his infirm health, and he was still in straitened circum-
stances in 1798 when he published a second edition of the
first part of his Ilistory. Ho also enlarged Ozanam's
Mathematical Recreations, afterwards published in English
by Dr Hutton (4 vols., Lond., 1803). About four months
before his death (December 1790) a pension of 2-100 francs
was conferred upon him. His History of Mathematics was
completed by Lalande, and published at Paris in 1799-1802
(•t vols. 4 to).
Jlontucla's work was the first history of mat}upiatics w-orthyof the
name. It is characterized alike by elegance of style and by breadth
of treatment- Montucla rarely fails iu candour, and never in breadth
of sympathy j he Bved at a time when it would have been pardon-
able to treat mathematics "as a French 'science," yet he cannot
with justice be accused of Chauvinism. The study of the history
of mathematics has greatly revived of late years, especially in
Germany, and numerous monographs on special departments have
appeared, iu w-hich, as was to be e.\pected, many defects and some
positive errors in Jlontucla's work have been pointed out, but,
taken as a whole, it stands as yet unsuperseded, unrivalled, fit, as
to its admirable stvie and endming quality, to bo compared with
Gibbon's Decline and Fall of the Jloman Empire.
MONZA (locally Monscia), a city of Italy in the pro-
vince of Milan, at the branching of the railway for Lecco
and Como, lies on the Lambro, a tributary of the Po,
mainly on the right bank, in a healthy and attractive
situation. Of the mediaeval fortifications little remains
save the Porta d'Agrate. The cathedral of St John
Baptist is the principal object of interest : Theodelinda's
basilica -was enlarged at the close of the loth century by
throwing the atrium into the main building, and the
present marble facade was erected about the middle of
the llth by Matteo da Campioue. On the left-hand
side of the front rises an incongruous brick-built to-wer,
278 feet high, erected by Peregrini. Within the church
are the iro-i crown of Lombardy (removed by Austria
in 1S59, and since restored) and the relics of Thcodelinda,
comprising her . cro-wn; fan and comb of gold, and the
golden hen and seven chickens, representing Lombardy
and her seven provinces. Next to the cathedral in artistic
importance come the church of Santa Maria in Istrada,
and the broletto or old palace of the commune, usually
styled the Arengario : the former (founded in 1357) has a
rich Bramantescjue fai;ade, reckoned one of the best pieces
of tcrra-cotta work in Lombardy, and the latter is raised
on a system of pointed arches, and has a tall square to-n-er
terminating in machicolations surrounding a sharp central
cone. San Jlichele -ivas the scene of the coronation of
Conrad III. in 1128, and San Gerardo (formerly Sant'
Arabrogio) is named after the patron saint of Monza,
Gerardo de' Tintori, who founded the first local hospital in
117-i. The royal palace of Monza (1777), with its exten-
sive gardens and parks, lies not far from the town on the
banks of the Lambro. Cotton goods and felt hats are the
staple products of Monza industry ; then dyeing, organ-
building, and a publishing trade. The population of the
city was 15, -150 in 1871, and that of the commune increased
from 24,661 in 1861 to 28,012 in 1881.
Local antiquaries claim for Monza {ilodicia or Modcetia) the rank
of a Roman colony, but it cannot have been a place of consequence
till it attracted the discerning eye of Theodoric ; and, though it was
a favourite residence with his immediate successors, its first im-
portant associations are with Thcodelinda {see vol. xiv. p. 815).
During the period of the republics Jlonza was sometimes inde-
pcndeut, sometimes subject to Mil.au. The Visconti, who ulti-
mately became master's of the city, built a castle in 1325 on the
site now occupied by the Palazzo Durini. In the course of its
history Monza has stood thirty-two sieges, and been repeatedly |>luu-
dered, notably by the forces of Charles V. The countship'(1499-
1796) was purchased in 1546 by the wealthy bauker Duriui, and
remained in his family till the Revolutio.n.
MOOLTAN. See Mi)lt.L\.
MOON, The. The subject of the moon divides itself
into two separate branches, the one concerned with the con-
stitution of the luiiar globe, the other w-ith its motions.
For the first subject the reader is referred to the article
AsTKONOMY (vol. ii. p. 801 sq.) ; the jire-sent article is con-
fined to the second, which is commonly called the Lvnar
Theory.
The kmar theory does not yet form a well-defined
body of reasoning and doctrine, like other branches of
mathematical science, but consists only of a series of
researches, extending through twenty centuries or more,
and incapable of being welded into n consistent whole.'
MOON
799
This state of things arises from the inherent difficulties
and complexities of the subject, and from the fact that no
one method or system has yet been discovered by which
all the difficulties can be surmounted and all the com-
plexities disentangled. Hence each investigator, when he
has desired to make any substantial advance beyond his
predecessors, has been obliged to take up the subject from
a noTT point of view, and to devise such method as might
seem to him most suitable to the special object in hand.
The historical treatment is therefore that best adapted
to give a clear idea of the results of these investigations.
Tlie ancient and modern histories of the subject are quite
distinct, the modern epoch commencing with Newton. The
great epoch made by Copernicus did not extend to the case
of the moon at all, because in every investigation of the
moon's motion, modem as well as ancient; the motion is
referred to the earth as a centre. Hence the heliocentric
system introduced no new conception of this motion, except
th.-\t of taking place round a mo^'ing earth instead of round
a fixed one. This change did not affect the consideration
of the relative motion of the earth and moon, with which
alone the lunar theory is concerned. The two stages of
the lunar theory are therefore — (1) that in which the treat-
ment was purely empirical, (2) that in which it was founded
rationally on the law of gravitation.
It is in the investigation of the moon's motion that the
merits of ancient astronomy are seen to the best advan-
tage. In the hands of Hipparchus (see Astronomy, vol.
ii. p. 749) the theory was brought to a degree of precision
wliich is really marvellous when we compare it, either
with other branches of physical science in that age, or
with the remarks and speculations of contemporary non-
scientific writers. Whether this was wholly the work of
Hipparchus, or whether he simply perfec'ted a system
already devised by his predecessors, it is now impossible to
say ; but, so far as certain knowledge extends, the works of
his predecessors did not embrace more than the deter-
mination of the mean motion of the moon and its nodes,
.^though the general fact of a varying motion may have
been ascertamed, the circiunstances of the variation had
probably never been thoroughly investigated. The dis-
coveries of Hipparchus were : —
1. The Ecceniriciiy of the Mooii's Orbit. — Ho found that
the moon moved most rapidly near a certain point of its
orbit, and most slowly near the opposite point. The law
of this motion was such that the phenomena could be re-
presented by supposing the motion to be actually circular
and uniform, the apparent variations being explained by the
hypothesis that the earth was not situated in the centre of
the orbit, but was displaced by an amount about equal to one-
twentieth of the radius of the orbit. Then, by a well-known
law of kinematics, the angular motion round the earth would
be most rapid at the point nearest the earth — that is, at
peri/fee — and slowest at the point most distant from the
earth — that is, at apogee. Thus the apogee and perigee
became two definite points of the orbit, indicated by the
variations in the angular motion of the moon.
2. The Motion of the Perigee and Apnf/ee. — As already
defined, the perigee and apogee are at t!ie ends of that
diameter of the orbit which passes through the eccentrically
situated earth, or, in other words, the)- are on that line
which passes through the centre of the earth and the centre
of the orbit. This line was called the line of apsides. On
comparing observations made at different times, it was
found that the lino of apsides was not fixed, but made a
complete revolution in the heavens, in the order of the
•igns of the zodiac, in about nine years.
3. The JTumerical Determination of the Elements of the
Moon's Motion. — In order that the two capital discoveries
just mentioned should have the highest scientific value it
was essential that the numerical values of the elements
involved in these complicated motions should be fixed with
precision. This Hipparchus was enabled to do by lunar
eclipses. Each eclipse gave a moment at which the longi-
tude of the moon was 180° different from that of the sun,
and the latter admitted' of ready calculation. Assuming
the mean motion of the moon to be known and the perigee
to be fixed, three eclipses observed in different points of
the orbit would give as many true longitudes of the
moon, which longitudes could be employed to determine
three unknown quantities — the mean longitude at a given
epoch, the eccentricity, and the position of the perigee.
By taking three eclipses separated at short intervals, both
the mean motion and the motion of the perigee would be
known beforehand, from other data, with sufficient accuracy
to reduce all the observations to the same epoch, and thus
to leave only the three elements already mentioned un-
kno-vvn. In the hands of a modern calculator the problem
would be a very simple one, requii-ing little more than the
solution of a system of three equations with as many un-
known quantities. But without algebra the solution was
long &nd troublesome, and not entirely satisfactory. Still,
it was probably correct within the necessary limits of the
errors of the observations. The same three elements being
again determined from a second triplet of eclipses at as
remote an epoch as possible, the difference in the longitude
of the perigee at the two epochs gave the annual motion
of that element, and the difference of mean longitudes gave
the mean motion. Such was the method of determining
the elements of the moon's motion down to the time of
Copernicus.
The determination of the eccentricity from eclipses, as above
described, leads to an important error in the resulting value of the
eccentricity, owing to the effect of tJie neglected erection. "We
know from' our modem theory that the two principal inequalities
in the moon's tnio longitude are —
6°-29 sin g (Equation of centre)
+ V-27 sia{2D-ci) (Evection),
where g = mean anomaly, and D = mean angular' distance of the
moon from the sun. Kow during a lunar eclipse ■n'e always have
Z> = IS0° very nearly, and ID = 360°. ^ Hence the evection is then
- 1'''27 sin ff, and so has the same argument, ff, as the equation of
centre, and so is confounded ivit<i it. The value of the equation
of centre derived fram ecliijses is thus (6°'29- 1°'27 = 5°'02) sin g.
Therefore the eccentricity lound by Hipparchus and Ptolemy was
only 5*, and was more than a degree less than its true value. '
The next important step in advance was the discovery
of the "evection," which is described by Ptolemy (see
Astronomy, vol. ii. p. 750) as if made by himself. In
view of the bad habit which Ptolemy had of making his
own observations verify results previously arrived at, which
were sometimes in error, we must view such a discovery
by him as quite exceptional, and as best explainable by the
large magnitude of the outstanding error. Although, as
just sho-ivn, the erroneous eccentricity found by Hipparchus
would always represent ecUpses, so that the error could
never be detected by eclipses, the case was entirely different
when the moon was in quadratm-cs. Comparing the in-
equalities already written with that found by Hipparchus,
we see that the latter required the correction —
r-27 {sin^-l-sin (2i)-jr)} =
r-27 {(1 -cos2i))siny + sin2i)cos^}
At quadratures we have D = ±90°,.2Z>= 180°, and hence
cos 2i) = - 1 and sin 22) = 0. The omitted inequalities
at these points of the orbit have therefore the value
2°-5-t sin y, a quantity so large that it could not fail to be
detected by careful observations ■n'ith the astrolabe. Such
an inequality as this, superposed upon the eccentric motion
of the moon, was very troublesome to astronomers who had
no way of representing the celestial motions except by
geometrical construction. The construction proposed by
Ptolemy was so different from those employed for the
800
M O 0 R
motions o!' lite plnnc-t^, and ■witlial so intricate, that little
interest attaches to it.
The student of Arabian science may find much to interest
him in the astronomical speculations of the Arnbs, but this
jieople do not seem to have [uruisUed anythii-.g in the way
of suggestive theory. In the fourth book of £>e Ecvolu-
iionihus,^ where we find the lunar theory of Copernicus, no
^vTiter later than Ptolemy is referred to. >Ioreover, as
already intimated, the Trork of Copernicus in this particu-
lar direction forma little more than an episode in the his-
tory of the subject. The working hj^othesi.s of the great
founder of modern astronomy was borrovrcd from the
ancients, and was that the celestial motions were all either
circular or compounded of circular motions. The hypo-
thesis of equal circular motions, though accepted by Ptolemy
in name, was so strained by him in its applications that
little was left of it in the Almag'M (the Arabic translation
of his St/ntaxis). But. by taking the privilege of compound-
ing circular motions indefinitely — in other words, of adding
one epicycle to another — Copernicus was enabled to repre-
sent the planetary and lunar inequalities on a uniform
system, though his heai-ens were perhaps worse "scribbled
o'er " than those of Ptolemy. To one epicycle representing
the equation of the centre he added another for the cvection,
and thus represented the longitude of the moon both at
quadratures and oppositions. But the third inequality,
"variation," which attains its maxima at the octants and
vanishes at all four quarters, M'as unknown to him. To
Tyeho Brahe is commonly and justly ascribed tha diseoveiy
of the variation. Joseph Bertrand of Paris has indeed
claimed the discovery for Abii 'I-WefA, an Arabian astro-
nomer, and has made it appear probable that Abii '1-Wefri
Really detected inequalities in the moon's motion which we
now know to have been the variation. But ha has not
.shov.Ti, on the part of the Arabian, any .such exact de-
scription of the phenomena as is necessary to make clear
his claim to ths discovery. A^ regards Tycho, although
he discovered the fact, ho could add notliing in the way of
suggestive theory. To the double epicycle of Copernicus
he was obliged to add a, motion of the centre of the whole
lunar orbit round a circle whose circumference passed
through the centre of the earth, two revolutions round
this circle being mnde in each luaation. Kepler, by intro-
ducing a moving ellipse having the earth as its fo.cus, was
enabled to make a nearer approach to the truth than any
of his predecessors. But the geometrical h}-potheses by
which he represented the inequalities due to the action of
ths sun form no greater epoch in the progress of science
than do the geometrical constructions of his predecessors.
Wo may therefore dispose of the ancient history of the
lunar theory by saying that the only real progress from
Hipparchus to Xewton consisted in the more exact deter-
luiuation of tho mean motions of the moon^ its perigee
and its line of nodes, and in the discovery of three new
inequalities, the representation 6f which required geometri-
cal constnictions increasing in complexity with every step.
Tho nioderu hmar theory commenced with Newton, and
consist ■; in determining the motion oY the moon deductively
from tho theory of gravitation. But the great founder of
modern mechanics did not employ tho method best adapted
to load to the desired result, and hWce his elT;>rts to con-
struct a lunar theory aro of more interest as illustrations
of his w-onderful power and correctness in mathematical
reasoning than as germs of new methods of research. Ho
succeeded perfectly in explaining tho elliptic motion of two
mutually attracting bodies round their common centre of
gravity by geometrical constructions. But when the prob-
' The full title, Dc P.fvnhttioiULita Orbium Calcslhtm Libri VI,
(email folio, Kurombei'g, 1543).
1cm was one of determining the variations from the elliptic
motion which would be produced by a third body, such
constructions could lead only to approximate results. The
path to modern methods was opened up by the Continental
matheuiaticiai;s, whoso great work consisted in reducing
the problem to one of pure algebra. Tho cha;;in between
the laws of motion laid down by Newton and a problem
of algebra seems so difficult to bridge over thst it is worth
while 10 show in what the real spirit of the modern metho.;
cousi.sts. We call to mind the statement of Newton's first
two laws of motion : that a body uninfluenced by any force
moves in a straight line and with uniform velocity for ever,
and that the change of motion is proportional to the forte
impressed upon tho body and in the directioji of such
force. These two laws admit of being expressed in alge-
braic language thus : — let us put m the mass of a material
point; X its distance from any fixed plane whatever; ;
the time ; X the sum of the components of all the forces
acting upon the point in the direction perpendicular to the
fLxod plane, it being supposed that each force is resolved
into three mutually perpendicular component.s, one of which
is perpendicular to the fixed plane ; then the differential
equation
<Px -,
expresses Newton's fir;/c tvro la,ws of motion with a com-
pleteness and precision which is entirely wanting in ail
statements in ordinary language. The latter can be no-
thing more than lame attempts to e."q5vess tho equation in
language which may be understood by the non-mathe-
matical reader, but which bear the same relation to the
algebraic equation that a statement of tho operations of
the Bank of England in the symbolic language of a tribe
of savages would bear to the bank statement in pound.';,
shillings, and pence. By taking two other planes, perpen-
dicular to each other and to the first plane, wo have three
equations like the one last written. The law of gravitation
and Newton's third law of motion enable us to substitute
for X and the other forces the masses and coordinates c!
the various attracting bodies. Thus the data of the problem
are expressed by a triplet of three equations for each attract ■
ing body. The integration of these equations is a problem t^f
pure algebra, which, when solved, leads to expressions thr ■
give the position of each body in terms of the time, whicl:
is what is wanted. The special form which it is necessary
to give the equations has not been radically changed durint-
the century and a half since tliis method of research wa.'-
opened out. Tlie end aimed at is the algebraic expression
of all the quantities involved in the form of an infinit-
series of terms, each consisting of a constant coefBcien;
multiplied by the sine or cosine of an angle increasiii;
uniformly with tho time. It is indeed a remarkable fa* :
that, notwithstanding tho great advances which moder.-
uiathematics has made in tho discovery of functions mo!'.
general than the old-fashioned sines and cosines of eh
mentary trigonometry, especially of elliptic functions, ye:
the form of development adopted by the mathematicians Oi
ths la.st century has remained without essential change.
It will bu iiistrHctive to ucticc tlio general and simple property
of the tiigonomctric fKnotious to which is due their great advaii-
t:ige ill the problcias of celestial me^^baiiics. It nijiy be exprcsscii
thus : — J/vc harr, any numlcr of qimiUilies, each ofichkh is a
nrcsscd iii the fiinii of a tn'goiioiiictrie series in whicli tJii angh-
increeiss niii/orudi/ with the ti^ne, then all the jioicers and yrodue! •
of these quantities, and all their ih'fcrcntiah and integrals v>il'<
respect to the time, may ie expressed in scries of the snmcfcnn. Tiii-
theorem needs ouly au illustration by an exnmplo. Let our quan-
tities be X and Y, and let U3 suppose them expressed in the form
X = a cos A + h cos JD + e cos C'+, kf.
Y—a' sin A' -¥1' sin E + c' ."in &+, kc,
in which we may suppose that the quantities a, h, e, kc, converge
towards zero. In forming their product, the first term wiU.bc
n o o is:
801
oa' cos A iia A', But tto hive cos v< sin ^'=i Bin (.'1' + ^;)
+ i sin (^' - A). HcEce ths product j: r will bo of the form
X r= i ««' siE (^' + ^) + 1 oa'sin {A' - A)-i-\aVsxn{A+Il' ^ ),&c.,
which is anotlier series of tbe samo general form. Moreover, if
■we siii/pose the angles A, B, &c., to increase uniformly with the
time— that is, to admit of expression in the form
we shall haTC, by integratini?,
"O' ,11 .^ L
r,cos;^-!-X)- ,_ cos(yi -A), &C,
2rzr<a=-~r^,'
which, again, is a trigonometric scries of the same general form,
which admits of being manipulated at pleasure in the same way
as the origijid cxoressious X and Y. This proper*)' does not
belong to the elliptic functions, and in conse<iuence, notwith-
standing the great length of the trigonomctiic series, no attempt
to supersede them has been successful.
The efforts to express the moon's motion by integrating
the differential equations of the djTiamical theory may bo
divided into three classes. (1) Laplace and his immediate
successors found the problem so complex that they sought
to simplify it by reversing its form ; instead of tiding from
the beginning to express the moon's coordinates in terras of
the time, they effected the integration by expressing the
time in terms of the moon's true longitude. Then, by a
reversal of the series, the longitude was expressed in terms
of the time. Although it would be hazardous to say that
this method is unworthy of further consideration, we must
admit that its essential inelegance is such as to repel rather
than attract study, and that it holds out no promise of
further development. (3) By the second general method
the moon's :oordinates are obtained in terms of the time
by the dire;t integration of the differential equations of
motion, retaining the algebraic symbols which express the
values of the various elements. Most of the elements are
small numerical fractions : e, the eccentricity of the moon's
orbit, about 0055 ; e, the eccentricity of the earth's orbit,
about 0'017 ; y, the sine of half the inclination of the moon's
orbit, about 0i)'16 ; m, the ratio of the mean motions of
the moon and earth, about 0'075 ; and the expressions for
the longitude, latitude, and parallax appear as an infinite
trigonometiic series, in which the coefficients of the sines
and cosines are themselves infinite series proceeding accord-
ing to the powers of the above small numbers. This
method was applied with success by Pontecoulant and
Sir John W. Lul.bock, and afterwards by Delaunay. It
should be remarked that the solution by the first method
appears in the same form as by this one after the true
longitude is expressed in terms of the mean longitude.
(3) By the method jjst mentioned the series converge so
slowly, and the final expressions for the moon's longitude
are so long and complicated, that the series has never been
carried far enough to insure the accuracy of all the terms.
This is especially tbe case with the development in powers
of m, the convergence of which has often been questioned.
Hence, when numerical precision alone is aimed at, it has
been found best to avoid this difficulty by using the
numerical values of the elements instead of their algebraic
symbols. This method has the advantage of leading to
the more rapid and certain determination of the numerical
values of the several coefficients or sines and cosines. It
has the disadvantage of giving the solution of the problem
only for a particular case, and of being inapplicable in
researches in which the general equations of dynamics have
to be a pplied. It has been employed by Damoiseau, Hansen,
and Airy.
The methods of the second general class are those most
worthy of study. And among these we must assign the
•rst rank to the method of Delaunay, developed in his
Thiorie du Mauvement de la Lune, because it contains a
germ which may yet develop into the great desideratum of
a general fnethod in celestial mechanics. To explain it,
we must call to mind the general method of " variation of
elements," due to Lagrange. This method is applicable to
cases in which a problem of dynamics can be completely
solved when any small forces which come into play are
left out, but which does not admit of direct solution when
these forces are included. Omitting the small forces,
commonly called " disturbing forces," let us suppose the
problem of the motion of a body under the influence of the
" principal forces " completely solved. This will mean
that we have found algebraic expressions for the coordi-
nates which determine the position of the body in terms
of the time, and (in the case of a material point) of six
constant quantities, to which 'we may assign values at
pleasure. Then Lagrange showed how, by supposing
these constant quantities to become variable, the same
expressions could be used for the case in which the effect
of the disturbing forces was included. In other words, the
effect of the disturbing forces could be determined by
assuming them to change the constants of the first approxi-
mate solution into very slowly varying elements.
In the researches on the lunar theory before Delaunay
the principal f oice was taken to be the attraction of the earth
upon the moon, and the disturbing force was that due to
the sun's attraction.. When the action of the earth alone
was included the moon would move in an ellipse, in accord-
ance with Kepler's laws. The effect of the sun's action
could be allowed for by supposing this ellipse to be mov-
able and variable. But when it was required to express
this variation the problem became excessively complicated,
owing to the great number of terms required to express
the sun's disturbing force. Now, instead of passing from
the elliptic to the disturbed motion by one single difficvilt
step, Delaunay effected the passage by a great number of
easy steps. Out of several hundred periodic terms, the
sum of which expressed the disturbing force of the sun,
he first took one only, and determined the variations of
the Keplerian ellipse on the supposition that this term
was the only one. In the solution the variable eleibents
of the ellipse would be expressed in terms of six new con-
stants. " He then showed how the.se new constants could
be taken as variables instead of the elements of the original
ellipse. Taking a second term of the disturbing force, he
expressed the new constants in terms of a third set of con-
stants, and so repeated the process until all the terms of
the disturbing force were disposed of.
Among applications of the third or numerical method,
the most successful yet completed is that of Hansen.
His first work appeared in 1838, under the title Funda-
matta nova investigationis orbitee vera quam luna perlustrat,
and contained an exposition of his ingenious and peculiar
methods of computation. During the twenty years follow-
ing he devoted a large part of his energies to the numerical
computation of the lunar inequalities, the re-determination
of the elements of motion, and the preparation of new,
tables for computing the moon's position. In the latter"
branch of the work, he received material aid from the
British Government which published his tables on their
completion in 1857. The computations of Hansen were
published some seven years later by the Saxon Royal
Society of Sciences.
It is found on Comparing the results of Hansen and
Delaunay that^ there are some outstanding discrepancies,
which, though too small to be of great practical importance,
are of sufficient magnitude to demand the attention of
those interested in the mathematical theory of the subject.
It is therefore desirable that the numerical inequalities
should be again determined by an entirely different method.
This is the object of Sir G. B. Airy's Mvtnerical Lunar
Theory, which is not yet completely published, but is
sufficiently far advanced to give hopes of an early comple-
tion. '^^ The essence of Sir George's method consbts in
10—29
«02
starting with a provisional approamate solution (that cf
Delaunay bemg accepted for the purpose) andlubs tutin.
me^tTSZi^^ ''^ -on's c'oor'dinairf; thf S
u uy ine sun. it the theory wera perfect the two
«des of each equation would come out equa '1^ thiy
in tne lorni. mat corrections must be applied to the
Te fouThl 1 ° '''°''" ^°'^ ''^^^^ corrections may
be found by solving a system of equations. ^
solvinl th„ ..? K f?- .■^° .°,"'" "^''■"<'^' the question is that of
el'IwfnnL^ f/,"!^ problem of three-bodies » ia the speci!
tKo her two and i,1'"' ""1™"' ''"^ " '""^'' S^^^'" ^^=^ ^an
they are fril'^^ ,^ " "^'n'' S"'""'" '^'''"'"™ f™™ them than
cney are from each other. All methods lead to a solution of tho
same geueral form which we shall now describe Lot us nut r the
£i5Meor£=— ^-SS
wio eaiti! and of the earth round the iun, while u> and 0,' r^m-^i^
InyTLJtr ''™^lf '^ '"''^" °f ''"^ ac'tiln of ae sun iS
quence ft e m "^' T' "^ r "f"^"™' r'-og.'essiye motion. lu cons"
movin'; emnf ^ '"'"' °^ "'' °'°°" "-"""d "'« '^"'h becomes a
SrS f„ Ihff ■^°'' "'J°' ""'^ ""kes a revolution round the
earth in about nine years, and the lino of whose nodes make, a
i-evolution m about eighteen and a half yeair All ?heon^,r?l«
^Z^^I^^^r^' "^ -^J- aSritsticentri: ; atd
?ni^tbe ^^? ' «=<^l'P"=-remain absolutely constant however
^a moon there are ,>ori?drc de'vir'Sns ffom hi^'e Upt"t"i:h mav
. ■; (sin or cos) {ig + ,y +_;■„ +_,■■„•)_
]VTtd^'JT^'"''"'r.^'^"'^''''^y '=™^'^"* coeffioients, and
-liiittve ^r^t^vl^Jr^ ?hY*t^:L"rr^^^^^^^^
Jo^%he^;:x^"fef„r^"nv^^^^^
L |p?:^n:Yi-g?^ij-.i^:t?x''oi^:te^t-5
the other odd m he case of the latitude. For examp™ if we sun-
pose J, J, and, aU zero, we shaU have terms of the form ^
c, sin </ f cj sin Zg' + Cj sin V + , ic.
fom '""" °'^" *'™'' '"PP°'' ' = ^' "'^" "■' h«™ to^s of the
e, sin (a-s'^ + c, .-ia (y + ;,•) + «, sin (g + 2g') + , &c.
MOON
discrepancy had to>e sought for. A probabir cai^w^ plted
ilterwards bv Delannav Ti,. f„_ —
the^m^ **"' '"'' ^'^<"'>=2 and /= -2, wo shall have' terms of
"hsin(i/-!/ + 2u,-2.,') + »Hsin(ff-2^ + 2<^-2a,') + , ic.
Jfer w"" ' V"' A """^-i' '""=°™'' '^''«"' "^0 coefficients c, e, m,
theonesol Hansen and Delaunay amount to several hundreds. In
dents" J rl r"''^ ''r° ?f- "/ ^"''''^"^y- ^^'^'> "^ *" ^^ffi'
cients c, cm, ic, 13 a co-r.,pheated mfinite series, but in the numerical
theones it is a constant number. And the principal probTem of
ffidrt Wea r:f,h '^r "^^^T '? "• «"<! the^ppr^oprlate co
emcient lor each ol thece hundreds of terms
AcUon of the Planets m. tlu: Moon.-For nearly two centuries it
has been known from observations that the mean motion of the
moon round the earth is not absolutely constant, as it on °ht to
be were there no disturbing body but the sun. The general fact
that the motion has been accelerated since the time of Ptolemv
was first pomteJ out by Halley, and the amount of the accelera bn
was found by Dunthorne. After vain efforts by the greatest ma he
matcians of the last century to find a physical cause for the
acceleration, Laplace was successful in tracing it to the secular
diminution of the occ.-ntncity of the earth's orbit, produced by the
action of tho planets. He computed its amount to be lo'' per
century— that is, if the place of the moon were calculated forward
on Its mean motion ; t the beriuning of any century, it would at
tlio end of tho century bo 10' in advance of its computed place
I his theoretical ivult of Laplaco agreed so closely with the
acceleration found by Lalando from the records of ancient and
niedia;val cclinses that it was not questioned for nearly a century
In 1652 llr John C. A.lams showed that Laplaco had failed to
iAo account of a scries of terms, the clTect of wliich was to reduce
out £st bv F .. 1 7*ff i°r. A probable causa was pointed
oui, nrst by t'errel, and afterwards bv Delaumv T),= iv.™
in papere published in Gould's MtronomimJouIn^r. A .■^'
t me. Since, as the days became longer, the moon would move
I rltX^ ■ """^ ^'T "" "PP"*^"' acceleration would be he?e°dt
That this cause really acts there can be no doubt. But the Jata
^p^l^ZlS-d"^J^-£i54!;£=?
the obseived acceleration to be accoimted for by the tidal JetprHr
tion amounts to onlv 2" twr ,.oT>t,„.„ "-u lui uy loe imai rctarda-
th;„ «^,ii 1 ^■' .™ centuiy, and may be even less But
S:;X"m=^^rs'u^;U\tlro7t^ol^^^^^
notably the echpse asL'ciated '^°S? V/ n m of'ISef *Thkl:
which had been predicted ty ThJes f the W , I "^f^'^'
efficient resulting' from the combined efi^ec of HM rl? 1 '^^ "",
the earth and secular acceleration of tt m„„n I 1 'Sn^lV
ni near the value found by Hansen from theon' and ad ' Zj'?''
pll£teal%Ze"^oY^hlt=itI^^^^^^
day to be constant, is, according to Ddaunay ! c"-] 76
Hansen s value, in his Tables de 1% Lmu, is la-iR
Hansen s revised but still theoretically erroneous resui't'is lo-jg
mnfT/V"''?o^?V'''P'''='^'"^ ^^ ^"PP-'^^'l eclipsed
Tifi I „T r '• '-> ^\ ^"'^' (^' =" Stikkefstad, is about 11 7
?|rplJ^Ztt^uZ^^t--;Sone "^
The n-oon lound rl"' ";r "^'™,S P"'°'^ ^ «1>^ »^» motion of
^™?sp'\,;f^„r'i„dis;:?\,-'ij--tjtir'^
^|:^™^p-L;-:-na-i-^/S}
in 183o, disputed the rea ty of the ineoualitv fint IwTt'
us discussion of the Greenwich obse'vXlif ietw" n"" -po'Z
1830, conclusively proved its existence. About the same «Sb
Hansen announced that he had found from O.cory two TeL^?
Z/^".°^.,''"""S '^'r ""^ ^'=«°" of Venus whch fully ™rre
sponded to the inequalities indicated by the observations Thl»
terms, as employed in hie Tables dc la Lnc, are
'?!,''?i ^;" (-?-16?' + 18<7" + 33° 36')
+ 21 -47 sin (8y'-13y'+4°44'),
' il^7^'''',V' ^'i i'."" "" "P'^'^sent the mean anomalies of the moon,
the earth, and A enus respectively. Durinu the first few v„„
after the publication of Hknsens tables they represented ohJII
tions so well that their entire correctne s^ argei^^allf t^ken
for panted. But donbt soon began to be thfo™ upon the
inequalities of long t>criod just mentioned. Indeed Hansen
himself admitted that tie second and lai-ger terra was par iy emrir"
cal being taken so as to satisfy observations between 1750 iid 1S50
Delaunay re-connvuted both terms, and found for the firsTterm a
result substantially identical with that of Hansen. But he f^nd
for he second or empirical one a coefficient of only 0" 27. S
would be quite insensi\,le. AVith this smaller coefficient tho ohs^T^
tions could go in deciding a purely mallieraatical question the
evidence was in fa^nr of Hansen's result. But oT compkr ng
Hansen 9 tables with observations between 1650 and 1750 it waf
found tliat the supposed agreement with observation was entire^
Illusory Moreover, since 1865 the moon has been steadily faSnK
behind the tabular, place. These inequalities of long period lav!
not yot been satisfactodly explained. The most plaufiKipposi
t.on ^ that they are'duo to tho action of one or more of the Tar^e;
planets. But the problem of the action of tho planX on the Zon
M 0 0 — M O O
803
ifl the most difficult and intricate of celestial mechanics, and do
Batisfactofy p-neral method of attacking it has yet beeu found.
The soarces of difl:"c;ilty are two in number. First, the disturbing
action of t'la planets is modified by that of the sun in such a way
that tha ordinary equations of disturbed elliptic motion aro no
longer rigorous, and hence new and more complicated ones must
be cccritructed. And, secondly, the combination of the four bodies
— moin, earth, sun, and planot — leads to terms so numerous and
intricate that it has haroly been found possible to isolate them.
The question has, indeed, been raised whether the rotation of the
earth on its iixis, and hence the unit of time, may not be subject to
slow and irregular changes of a nature to produce apparent corre-
Sjwnding changes in the motion of the mocn. Blit it has recently
been (bund, from a discussion of the observed transits of Mercury
since 1677, that, although such inequalities may exist, they cannot
have the magnitude necessarj' to account for the observed changes
of long period in the moon's motion.
The following is a summary of the present state of the various
ai-anshes of the lunar theory. (1) The numerical solution of the
problem of the sun's action on the moon may be regarded as quite
satisfactory, at least when Hansen's results shall have been veiified
by an independent method. (2) Tlie analytic theory needs to bo
perfected by finding some remedy for the slow convergence of the
series by which it is expressed, but its general form may be regarded
as quite satisfactory. (3) .Except in one or two special cases, the
action of the planets on the moon, when treated with the necessary
rigour, is so intricate that no approach to a satisfactory solution
has yet been attained. "When this desideratum is reached, the
mathematical theory will be complete. (4) The general discussion
of ancient and modern observations with a view to finding what
real or apparent inequalities of long period in the mean motion may
exist is stiU to be finished. 'With it the astronomical theory will be
complete. (S. N.)
MOORCROFT, William (c 1770-1825), traveUer in
Asia, was bora in Lancashire, about 1770. He was edu-
cated as a surgeon in Liverpool, but on completing his
•ourse he resolved to devote himself to veterinary surgery,
and, after studying the subject in France,began its practice
in London. In 1 795 he published a pamphlet of directions
for the medical treatment of horses, with special reference
to India, and in 1800 a Cursory Account of the Methods of
Shoeing Horses. Having been offered by the East India
Company the inspectorship of their Bengal stud, Moorcroft
left England for India in 1808. Under his care the stud
rapidly improved ; in order to perfect the breed, he resolved
to undertake a journey into Central Asia to obtain a stock
of Turcoman horses. In company with Captain William
Hearsay, and encumbered with a stock of merchandise for
the purpose of establishing trade relations between India
and Central Asia, Moorcroft left Josimath, well within the
mountains, on 26th May 1812. Proceeding along the valley
of the DauU, they reached the summit of the frontier pass
of Niti on 1st July. Descending by the towns of Daba
and Ghortope, Moorcroft struck the main upper branch of
the Indus near its source, and on 5th August arrived at
the sacred lake of Manasarowara. Returning by Bhutin,
he was detained some time by the Giirkhas, and reached
Calcutta in November. This journey only served to whet
Moorcroft's appetite for more extensive travel, for which
he prepared the way by sending out a young Hindustani,
who succeeded in making very extensive explorations. In
company with this young man and George Trebeck, Moor-
croft set out on his second journey in October 1819. His
enterprise was looked upon rather coldly by the directors,
who merely allowed him his pay for a time, all the expenses
being borne by Moorcroft himself. By way of Almori Snd
Srlnagar, Lahore was reached on 6th May 1820. On 14th
August the source of the Biyah (Hyphasis) was discovered,
and subsequently that of the Chenib. Leh, the capital of
Lad.lk, was reached on 24th September, and here several
months v.ere spent in exploring the surrounding country.
A commercial treaty was concluded with the Government
of Laddk, by which the whole of Central Asia was
virtually opened to British trade. Kashmir was reached
on 3d November 1822, and by the P(r Panjil mountains
JalAldbad on 4th June 1824, Cabul on 20th Ji'ije, and by
Khulm, Kunduz, and Balkh Moorcroft arrived at Bokhara
on 25th February 1825. Everj'where he bought horse.'*
for the company, and endeavoure.'l to establish trade
relations. At Andkho in Cabul Moorcroft was seized
■n-ith fever, of which he died on 27th August 1825, Trebeck
s'orviving him only a few days. It was not till several years
afterwards that his papers were obt.->,iaed by the Asiatic
Society, and published under the editorship of Horace
Hayman Wilson in 1841 under the title of Travels in the
Himalayan Provinces of Hindustan and the Pitnj&b, in
Ladakh and Kashmir, in Peshawnr, Kabul, Kunduz, and
Bokhara, from 1819 to 1825. Though published so long
after the traveller's death, the narrative was a valuable
contribution to a knowledge of Central Asia, and still
remains a classic. In vol. xii. of Asiatic Researches will
be foimd an account by Moorcroft of his first journey, and
in the Transactions of the Royal Asiatic Society, vol. i., a
paper on the Purik sheep.
MOORE, Edwajrd (1712-1757), minor poet, dramatist,
and miscellaqeous writer, was the son of a dissenting minis-
ter of Abingdon, vrhere he was born in 1712. He was the
author of the thrilling domestic tragedy of The Gamester,
originally produced in 1753 with Garrick in the leading
character, and still in the repertory of acting plays. It is
perhaps the strongest lesson against gambling ever preached
from stage or pulpit. The literary merit of the play is not
great, but it is powerfully constructed and fuU of impressive
incident, and the career of Beverley the gambler (a character
modelled on Fielding's Captain Booth) affords great scope
for the actor. Moore also wrote two comedies. As a poet
he produced clever imitations of Gay and Gray, and
with the assistance of Lj'ttelton, Chesterfield, and Horace
Walpole conducted The World (1753-57) during the great
decade of the revival of periodical essay- writing. The World
followed Johnson's Rambler, and was followed by The Idler ;
it had as rivals The Adventurer and The Connoisseur. Moore
died at London in 1757.
MOORE, Dr John (1730-1802), bom at Stirlingin 1730,
was one of the most prominent writers of travels and novels
in the latter part of the 18th century. His novel Zeluco
(published in 1789) produced a powerful impression at the
time, and indirectly, "through the poetry of Byron, has left
an abiding mark on literatiu'e. 'The novel would in these
days be called a psychological novel ; it is a close analysis cf
the motives of a headstrong, passionate, thoroughly selfish
and dnprincipled profligate. It is fuU of incident, and tiie
analysis is never prolonged into tedious reflexions, nor
suffered to intercept the progress of the story, while ths
main plot is diversified with many interesting episode.^.
The character took a great hold of Byron's imagination,
and probably influenced his life in some of its many moods,
as well as his poetry. It is not too much to say that the
common opinion that Byron intended Childe Harold as a
reflexion of himself cannot be cleared of its large mixture
of falsehood without a study of Moore's Zeluco. BjTOn
said that he intended the Childe to be " a poetical Zeluco,"
and the most striking features of the portrait were un-
doubtedly taken from that character. At the same time
it is obvious to everybody acquainted with Jloore's novel
and Byron's life that the moody and impressionable poet
often adopted the character of Zeliico, fancied himself and
felt himself to be a Zeluco, although he was at heart a
very different man. Moore's other works have a less
marked individuality, but his sketches of society and man-
ners in France, Germany, Switzerland, Italy, and England
furnish valuable materials for the social historian. Like
his countrymen Burnett and Boswell, he was a sagacious,
I penetrating, and in the main unprejudiced observer, with
I or.j-.otV.-'na' of a. natural historian's interest in the human
r suecies ; and he had exceptional opportunitiesof observation.
804
M 0. 0 E E
He was a doctor by profession, and the son of a Stirling-
shire ciergyman. After taking his medical degree at
Glasgow, he served with the army in Flanders, then was
attached to the household of the English ambassador at
Paris, then practised for five years in Glasgow, next
travelled on the Continent for five years with a young
nobleman, settled for some years as a physician in Lon-
don, accompanied Lord Lauderdale to Paris in 1792 and
witnessed some of the principal scenes of the Revolution.
All classes thus came under hia obser^'ation, while his pro-
fession preserved him in an xmusual degree from flippant
bias. His works attest great shrewdness and sagacity of
judgment, and show no small skill in literary presentation.
He died at London in 1802.
MOORE, Sir Jon^r (1761-1809), the ocly EngUsh
general who has gained lasting fame by the conduct of a
retreat, w.as the sou of Dr Moore (the subject of the pre-
ceding notice), and was born at Glasgow on 13th November
1761. It wa.", his appointment as tutor to the yOung duke
of Hamilton which procured for John Moore educatic::al
advantages by which ho profited so much as to bs called
in after life the most cultivated oiEcer in the army. It
was then the fashion, for young noblemen to travel from
court to court, and Moore accompanied his father and the
duke to all the chief capitals in Europe, until he was
suddenly ordered in 1777 to join the 51st regiment, in
which he had been appointed an ensign. He learned his
drill at Minorca, and in 177C was appointed lieutenant and
paymaster in a new regiment recenthr raised by the dulce
of Hamilton, with wljich he served in America till the peace
of 1783. In 1781 Moore, though but twenty-three years
of age, was returned by the duke of Hamilton as member
of parliament for the united boroughs of Selkirk, Peebles,
and Linlithgow. In parliament he does not seem to have
opened his mouth, though he always voted with the Govern-
ment ; but he made some aseful friends, notably the duke
of York and Pitt. In 1788 he was promoted to a majority
in the 51st regiment, and in 1790 he became lieutenant-
colonel and resigned his seat in parliament. He soon got
his regiment in fine order, and in 1792 sailed with it for
the Mediterranean. He was too late to assist at Toulon,
but was engaged throughout the operations in Corsica, and
especially distinguished himself at the taking of Cah'i.
After the expulsion of the French, Jloore became very in-
timate with Paoli and many of the leading Corsican patriots,
which intimacy was so obno.xious to Sir Gilbert Elliot, the
viceroy, that Moore was ordered to leave the island in forty-
eight hours. Sir Gilbert's hasty conduct by no means met
with approval in LonHon, and Moore was gazetted briga-
dier-general, and ordered to proceed with his brigade to
the West Indies. In April 1796 he readied Barbados,
and at once became the right hand of Sir Ralph Aber-
cromby, the command#r-in-chief. The first enterprise was
the reconqucst of the island of St Lucia, which was com-
pletely occupied by an agent of Victor Huguos with a
mixed force of Caribs, negroes, and Frenchmen. The key
of the island was a fortified and almost impregnable Iieight
called the Mome Fortune, which was at last stormed, tliough
with great loss, by the valour of brig.adier-geneial.^ Moore
and Hope, who were to bo comrades on a yet more memor-
able field. After this success, Sir Ralph left the island,
and appointed Moore governor and commander-in-chief.
A difficult post ho found his government, owing to the
swarms of Caribs and negroes in the woods ; but just as
he was on the point of triumphing he fell ill of yellow fever,
and wiV ordered home. In 1798 he was well and again
eager t(Jbe on active service, and he accompanied his friend
Abercromby over to Ireland, where he received the com-
mand of tlie Bandon district. In the Irish rebellion of
1798 he distinguished himself by his activity in saving
Wezford from destruction after the battle of Vinegpj Hiff,
His services were in universal reqirest, and Aberorocaby
insisted upon his sers'ing with him in the expedition to the
Helder in 179S, where he did creditably all that wascredit;-
ably done in that ill-managed expedition. On his retxira
from EoUand he was n-.ide colonel of the 52d regiment,
and in 1800 accompanied Abercromby to the Mediteirauean
as major-general.
Thj;onghout the Egyptian expedition he commanded the
reserve, and especially distinguished himself at the battle
of Alexandria, when he was wotmded in three placo.% and
behaved with such distinction that he was recognized uui-
versally as the greatest English general, now that Aber-
cromby was gone. The short interval of the peace of
Amiens did not ii jure Moore's prospects, and in 1 803 he
was appointed commandant of the camp at Storncliffe.
Here he proved his gi'eatness as an organizer, for it was
at this time that he organized those light regiments which
wei-e to form the reserve in his own campaign and the
light division in the Peninsular War. While at Shomcliife
he renewed his intimacy with Pitt, who was then residing
at Walmer Castle, and who on his return to oiBce made
Moore a knight of the Bath, and consulted him on every
military project. Fox, when he succeeded to office, showed
the same appreciation of Moore, and in May 1806 appointed
him second-in-command to his brother, General Fox, who
was ordered with a strong force to Sicily to supersede Sir
Jehu Stuart. MoOre won but little credit at this time, for
there was none to gain, but employed his time, according
to Napier, in falling in love with Miss Fox, to whom,
however, he never proposed, fearing to be accepted for h is
Dosition and not for himself. In 1807 he was able to escaiie
from the intrigues of the Sicilian court, and was ordered
to Portugal, which he reached too late to make any defence
of Lisbon, already in the possession of the French. He
then went home, and had four months' rest, the last he
ever had. In May 1808 he was ordered with a force. of
11,000 men to Sweden to assist the king against the united
forces of France and Russia. The mad conduct of the
Swedish king, however, who even went so far as to declare
Sir John Moore under arrest when he refused to acquiesce
in his pla.ns, ruined any chance of successful co-operation,
and the English general made his escape and returned to
England. He was at once ordered to proceed with his
division to Portugal, where Sir Arthur Wellesley had
already landed; but the appointment of Dairymple and
Burrard to the chief commands was even more of a slight
on Moore as a general of European experience than on
Wellesley, whose laurels had hitherto been won in India.
He regarded himself as personally insulted by the ministers,
and especially by Lord Castlereagh, but deemed it his duty
to go where he was ordered. He met his re^l■ard ; for when,
after the excitement caused by the Convention of Cintra,
Dairymple and Burrard went home, he was left in com-
mand of the largest English army since the commencement
of the war. Wellesley had appreciated him, and in an
interesting letter (pubUshed in the Wellington Despak-hes)
had expressed his desire to use his own great political
influence to reconcile him to the ministers and the minister.'!
to him
Now began the glorious three months on which Moore's
reputation as a soldier and a statesman must rest. The
Spaniards, flushed with their former success at Baylcn,
regarded Napoleon, \yho had in person crossed the PjTenees,
as another Dupont, and loudly summoned Moore to a share
in their coming victories. Jloore knew better what was
the value of Napoleon's genius, but he had been commanded
to assist the Spaniards, and therefore gave the order to
advance. His army marched in four distinct divisions,
and on 13th November 1808 he coucectrated at Salar
MOOR E
805
manca, -wliere Tie waited to see What would Lappen. He
heard that a subsidiai'y force under Sir David Baird
ha.l arrived at Conmna, and ordered it up to join him.
At Salamanca he rsmained a whole monlh watching the
{riiiMiphant successes of Napoleon and his lieutenants, and
learning how little Spanish reports or Spanish valour were
to be relied on. Though irritated by the menaces and
abuse of Frere, the English minister to the junta, he
waited till the 13th D-ecember, hearing daily of Spsinish
defeats, and then he determined to drav/ off upon his own
small force the weight of Napoleon's power, and thus give
Andalucia the winter in which to organize an army and
prepare for another Baylen. With this intention he
advanced through Toro and Mayorga, where Baird joined
him, to Sahagun. He judged rightly that Napoleon would
never advance into Andalucia and leave the English behind
him, but that he would turn all his power against them.
Having once drawn Napoleon's attention to hiciself, he
began his famous retreat and fell back quickly, fighting
every day and invariably with success. He now could
test the military spirit he had taught at Shomcliffe, for
the reserve under Sir Edward Paget consisted entirely of
his own light regiments. To detail each step of the retreat
and every skirmish would be but to rewrite Napier ; suffice
it to say that, with great loss of life and material, Moore
reached Corunna on 12th January 1809. But the fleet to
take the army home was not there ; and the English would
have to fight Soult, whose army was even more weakened
and demoralized than Moore's, before they could embark.
It was on 16 th January that Moore fought his last battle ;
he foil early in the day, and knew at once that his wound
was mortal. His last hours were cheered with the know-
lediSjc. of victory, but were spent in recommending his old
friends, such as Graham and Colbome, to the notice of the
Government. Sir H. Hardinge's description of these hours
is in its way inimitable, and in it must be studied how
a modem Bayard should die in battle, every thought being
for others, none for himself.
It may be possible in the face of his hei'oic deatli to exaggerate
>loore'8 actual military services, but his influence on the Briiish
army cannot be overrated. The true military spirit of disciuline
and of valour, both in officers and men, b^d become nearly extinct
dm*iag the American war. Aborcromby, who looked bacV to the
traditions of Minden, was the first to attempt to revive it, and his
worfe was carried on by Moore. The formation of the light regi-
ments at ShomclifTe was the answer to the new French tactics, and
it was left to Wellington to show the success of the experiment.
Moore's powers as a statesman are shown in his despatches written
ot Salamanca, and he had t!io truest gift of a great man, th,at of
judgin" men. It may be noticed that, while V/cUington perpetually
c.-unibled at the bad qualities of his officers and formed no school,
Moore's name is associated with the career of all who made their
mark. Among generals, Hope, Graham, Sir E. Paget, Hill, and
Craufurd, all fell and submitted to his ascendency, and of younger
oIlici-TS it was ever the proud boast of the Napicrs, Colborr.c, the
Beckwiths, and Barnard that they were the pupils of Moore, not of
Wellington. Nay more, he inspired an historian. The description
of Jloore's retreat in Napier is per'naps the iinost piece of military
history in the English language, not only because the author was
present, but because his heart was vnlh the leader of that retreat ;
and, if Napier felt towards Wellington as the soldiers of the tenth
legion felt towards C.Tsar, he felt towartis Moore the personal love
and devotion of a cavalier tow.irds Montrose.
The great authority for iloorc'a life is the Lifi ff Sir John Mo&rt, by !iis
brother, J. 0. Moore (1833) ; see also SarrcUive 0/ the Conpniyji of Sir JoSn
Jlfoore in Spain, by his brother, J. C. Moore (4to, with pUn% 1&09) ; Napier,
Penlnt^tlar War, Bk. iv., anU his Lift of Sir CharUa Napier. For views advert
to Moore's retreat, see Charrailly, Narrative (1810), and Sir Battle Frere, tVA'
0/ tiie JU. Hon. J. //. Frere (published in vol. i. of his worlis). Consult also
Wilson, Campaign in E^ypt, for Moore's services there, and the Life of Giltur:
Elliot, First Lord IJinto,~toT the squabble in Corsica. (H. M. S.)
MOORE, Thom.^s (1779-1852), bcm at DubUn on 2Sth
May 1779, faiily shares with Lord Byron the honour of
beiiig the most popular "poet of his generation. Whatever
may be thought now of the intrinsic qualities of his xeiso,
this much cannot be denied. The most trustworthy of all
measures of popularity is the price put upon a ■ .-ritei 's work
in the publishing market, and when Moore's friend Porry,
in negotiating the sale of the unwritten Lalia Rookh,
claimed for the poet the highest price thai had up to that
time been paid for a poem the publisher at once assented.
Moore was then in the heyday of his reputation, but twenty
years later publishers were still willing to risk their thou-
sands on his promise to produce. Much of Moore's success
was due to his personal charm. This at least gave him
the start on his road to popularity. There is not a more
extraordinary incideni in the history of our literature than
the instantaneousness with which the son of a humble
DubUn grocer 'just out of his teens, on his first visit to
London, captivated the fashionable world and established
himself in the couise of a few months as one of its prime
favourites. The youth crossed St George's Channel in"l799
to keep terms at the Middle Temple, carrying with him a
translation of the Odes of Anacreon, which he wished to
publish by subscription. Li a very short time he had
enrolled half the fashionable world among his sub.scribers,
and had obtained the permission of the prince of Wales
to dedicate the work to him. The mere power of writing
graceful and fluent amatory verses would not alone have
enabled the poet to work this miracle. Moore's social gifts
were of the most engaging kind. He charmed aU whom he
met, and charmed them, though he was not a trained
musician, with nothing more than with his singing of hi^i
own songs. The piano, and not the harp, was his instru-
ment, but he came nearer than anybody else in modem
times to Bishop Percy's romantic conception of the minstreh
To find a parallel to him we must go back to the palmy days
of Provenfal song, to • .such troubadcntrs and jonr/lettrs as
Axnaud Daniel and Perdigon, whose varied powers of
entertainment made them welcome guests wherever they
went. It was not merely the fashionable world that the
young adventujer captivated ; the landlady of his lodgings
in London, a countrywoman of his o^vn, offered to place at
his disposal all the money of which she had the command.
The fragment of autobiography in which Moore draws
a softly-coloured picture of his early life in Dublin lets us
into the secret of the seeming miracle of his social con-
quest. Externals apart, the spirit of his social surround-
ings in Little Aungier Street had much in common with
the society to which he was introduced in London. He
was born in the proscribed sect of Catholics, whose exclu-
sion from the society of the Castle produced a closer union
among their various ranks, and thus, from the first, Moore
was no stranger to the more refined gaieties of social inter-
course. It was, upon the whole, a gay life in Catholic society,
though the conspiracy of the United Irishmen was being
quietly formed beneath the surface. Amateur theatricals
was one of their favourite diversions, and gifts of reciting
and singing were not likely to die for want of applause.
Moore's schoolmaster was a leader in these entertainments,
a writer of prologues and epilogues and incidental songs;
and at a very early age Master Thomas Moore was one of his
show-boys, ardently encouraged in all his exercises by a very
affectionate mother at home. Before he left school he
had acquired fame in his own circle as a song- writer, and
had published, in the Anthologia Eibemica, verses "to
Zelia on her charging the author with vaiting too much
on love.'.' This was in 1793. In that year the prohibition
against Catholics entering Trinity College was removed,
and nest year Moore took advantage of the new freedom.
As one of the first Catholic entrants, he had an exceptional
stimijlus to work, and there industriously acquired that
classical scholarship with which he won the hearts of such
learned A\'higs as Lan'?do\vne and Holland, while he
charmed fashionable ladies >rith the grace of his songs.
Young Moore's .social atmosphere was, of course, strongly
charged with patriotism and hatred of the excesses of
806
MOORE
English despotism. Some of his closest friends in Trinity
were deep in the conspiracy of 1798. But even for his
patriotism — a genuine passion which he never sought to
disguise — Mooie • found plenty of sympathy among the
Whig political leaders, when he made their acquaintance in
the first years of the century.
Moore was fairly established in London society in the
£r3t year of ' -e century, and from that time the hope of
!its applause was the ruling aspiration of his life and its
(judgment the standard of his work. In his letters to his
mother, which are delightful prose lyrics and show the
most charming side of Moore's character— he wrote to her
constantly and with warm aflfection in his busiest weeks —
we find him, even in 1800, declaring himself surfeited
with duchesses and marchionesses, and professing his
readiness at any moment to exchange all his fineries for
Irish stew and salt fish. But he never did make the
exchange, even for more potent attractions than the fare
of his youth. Ho could not bear the shortest banishment
from fashionable dra\ving-rooms without imeasy longings.
The dignity and ease, the luxury, the gaiety, the bright-
ness of fashionable life, whoUj' satisfied his joyous and self-
indulgent nature. When men of rank com-ted his company,
when princesses sang his songs and peeresses wept at them,
Moore was too frank to affect indifJ'ereuce ; he was in the
highest heaven of delight, and went home to record the
incident to his relatives or transmit it to posterity in his
diary. If prudence whispered that he was frittering away
his time and dissipating his energies, he persuaded him-
self that his conduct was thoroughly worthy of a solid
man of business: that to get a lucrative appointment from
his political friends he must keep himself in evidence,
and that to make his songs seU he must give them a start
with his o\vn voice. But his mind was seemingly not;
much troubled either ■ivith sordid care or with sober pru-
dence ; he lived in . the happy pi'esent, and he Liked
fashionable company for its own sake, — and no wondej,
seeing how he was petted, caressed, and admired. Swift's
saying that great men never reward in a more substantial
way those whom they make the companions of their pleasures
was often in Moore's mind. It..was verified to some extent
in his own case. Through Lord Moira's Influence he was
appointed registrar of the admiralty court in Bermuda in
1803. He went there to take possession, but four or five
months of West India society, jingling pianofortes, and
dusky beauties bored him excessively, and he appointed a
deputy and returned to London, after little more than a
year's absence. The office continued to bring him about
.-S400 a year for fourteen or fifteen years, but at the end
of that time embezzlement by the deputy, for whom he was
responsible, involved him in serious embarrassment. This
was all that Moore received from his gTeat political friends,
— no gi'eat boon as things went in the days of patronage.
He had hopes from Lord Moira in the Gren%Tlle ministry
in 1806, — hopes of an Iri'^h commissionership or something
substantial, but the king's obstinacy about Catholic emanci-
pation destroyed the ministry before anything worth having
tm-ned up. The poet's long-deferred hopes were finally
extinguished in 1 8 1 2, when Lord iloira, under the Liverijool
administration, went out as governor-general to India
without making any provision for him. .From that time
Moore set himself in earnest to make a living by literature,
his responsibilities being increased by his marriage in 1811.
Fi-om his boyhood to 1812 may be called the first period
of Moore's poetical activity. He had formed the design
of transkiting Anacreon while still at college, and several
of the pieces published in 1801 under the nom de plume
of "Thomas Little" were written before he was eigMccn.
The somewhat ostentatious scholarship of the notts to his
Anacrco?!, the parade of learned rfuthorities, he exulair.ed
by his habit of omnivorous reading in Trinity College
library. Throughout his Uterary life he retained this habit
of out-of-the-way reading and clever display of it. Moore
had r'^ally abundance of miscellaneous scholarship as well
as great quickness in the analogical application of his
knowledge ; and, though he made sad havoc of quantities
when he tried to write in Greek, there was probably no
scholar of his time who woidd have surpassed him in the
interpretation of a difficult passage. He seems to have
spent a good deal of time in the libraries of the great
houses that he frequented; Moira, Lansdowne, and Holland
were all scholarly men and book-collectors. It might be
asked, — What had " pa-ssion's warmest child," whose " only
books were women's looks," to do with obscure mediaeval
epigrammatists, theologians, and commentators? But it
would seem that Moore took the hints for many of his
lyrics from books, and, kno'wing the gTeat wealth of fancy
among medifeval Latinists, turned often to them as likely
quarters in which to find some happy word-play or image
that might serve as a motive for his muse. The pubUc,
of course, were concerned with the product and net with
the ijrocess of manufacture, and " Little's " songs at once
became the rage in every drawing-room. He found his
songs in Virginia when he landed there on his way to
Bermuda. And not only were his songs sung but his
poems were read, passing rapidly thi-ough many editions.
The bulk of them were simple fancies, gracefully, fluently,
and sometimes wittily expressed, the lyrist's models being
the amatory poets of the 17th century from Carew
to Rochester. Carew is- the only eminent poet of that
century with whom Moore wiU bear comparison. The
highest praise that can be given to his amatorj- lyrics is
that he knew his audience, wrote directly for them, and
pleased them more than any of his competitors. Hi."!
publication of- 1806 was savagely reviewed in the Bdin-
lurgh by Jeffrey, who accused hini of a deliberate design
to coriTipt the minds of innocent maidens with his wanton
fe^ncies, and who had in consequence to figui'e in a ludicrous
attempt at a duel — ludicrous in its circumstances, though
Moore was ferociou.sly in earnest. We may well acquit
Moore of the diabolic intention attributed to liim, but
JeSrey's criticism of his poetry as poetry v.as just enough.
The only parts of the volume that Jelfrey praised were
the satu-ical epistles. The vein essayed in • these epistles
Moore pureued afterwards in his Corruption, Intolerance
(ISOS), and The Sceptic, a philosophical satire (1809) ; but
as long as he kept to the heroic couplet and the manner
of Pope he could not give full scope" to his peculiar powers
as a satirist. It may be remarked in passing that the result
of the hostile meeting with Jeffrey is a striking evidence
of the impressi veness of iloore's personality ; in the course
of a few minutes' conversation he changed a bitter critic
into a lifelong friend. Of all the poetical enterprises that
Moore undertook, either at this period or later, none was
so exactly suited to his powers as the task proposed to him
by the publisher Power of supplying fit words to a collection
of Irish mc'odies. The first number appeared in 1807, and
it was so successful that for twenty-seven years afterwards
■(vriting words to music was one of Moore's most regular
occupations and his steadiest soui'co of income. Power pay-
ing him an annuity of ,£500. Six numbers of Irish melodies
were published before 1815 ; then thoy turned to sacrod
songs and national airs, issuing also four more numbers of
Irish melodies before 1831. Moore entered into this work
with his best and most practised powers and ■nith all his
heart. From his boyhood he had been in training for it.
The most characteristic moods of Irish feeling, grave and
;;ay, plaintive and stirring, were embodied in those ail's,
and their \ariety touched the whole range of Moore's sensi-
tive ^piritj-carrying him far beyond the shallows of hiK
MOORE
807
spunous Anarrcontic sentiment, namby-pamby when not
prurient; lie wrote witli full inspiration, unresfrveJ sin-
cerity, and thoroughly roused faculty. Divorced from the
music, many of them are insipid enough, but they were
never meant to be divorced from the music ; the music
was meant, as Coleridge felt when he heard them sung by
the poet himself, to twine round them and overtop them
like the honeysuckle. Moore accomplished this with
exquisite art. His most conspicuous failures may be
traced to his habit of taking as his starting-point not an
emotional incident but some unmanageable intellectual con-
ceit. Hence arose intellectual discords, incongruous and
imperfectly harmonized fanci&j, which even the music can
hardly gloss over.
The regent's desertion of the Whigs in 1812 cut them
off from all hope of office for many years to come, and
Jloore from his last hoj-ie of a snug sinecure, -shen Lord
iloira also was practically " oblivioiis " of him. There was
at once a marked increase in his literary fertility, and he
broke ground in a new field, which he cultivated with
pre-eminent success — political squib-writing. Moore was
lEiOapablo of anything like rancour, but he felt the dis-
appointment of his hopes enoui;;h to quicken his fancy and
sharpen the edge of his wit. The prince regent, his old
friend and patron, who was said to have begged all Lord
Moira's appointments for personal favourites, was his first
butt. The prince's defects and foibles, his fatness, his
huge r/hiskers, his love for cutlets and cura(;oa, for aged
mistresses and practical jokes, were ridiculed with the
lightest of clever hands. Jloore opened fire in the Morning
Chroiivh, and crowned his success next year (1813) with
a thin volume of " Intercepted Letters," The Tviopenny Post
Bay. A very little knowledge of the gossip of the time
enauhi us to understand 'he delight with which Moore's
sallies were received in the year which ivituesscd the
imprisonment of Leigh Hunt for more outspoken attacks
on the regent. Moore received every encouragement to
work the new vein. He was at one time in receipt of
a regular salary from the Timts ; and his little volumes
of squibs published at intervals, — The Fudge Family
ill Pans, !S1S; The Jojirnal of a 2Iembcr of the Pococurante
Soci^ii.; 1620; Fable-f /or the Eoly Aliiance, 1823; Odes
on Cxsh, Com, Cuihottcs, and otlicr .Hatters, 1828 ; The
Fudjes in, Fiigland, 1835— went through many editions.
Tlie prose Ifemotrs of Captain Rock (1S24) may be added
to the list. Moore's only faihire was Tom Cribh's JUemorial
to Congress (1819), for which he had made an elabora^te
study of thieves' slang. It was of course on the side of
the TMiigs that Moore employed his pen, and his favourite
topics were the system of repression in Ireland and the
disabilities of the Catholics. He made rather too serious
a claim for his pasquinades when ho spoke of " laying the
lash on the back of the bigot and the oppressor." It was
not exactly a lash or a scoiu-ge that he wielded. It was
in happ}', airily malicious ridicule of personal foibles that
his strength lay ; he pricked and teased his victims with
sharp and tiny arrows. But, light as his hand was, he was
fairly entitled to the enthusiastic gratitude of his country-
men for his share in effecting Catholic emancipation.
The disappointment of 1612, which started Moore on
liis career as a squib-writer, nerved him also to a more
sustained effort in serious verse th.in he had before at-
tempted. Lall'i Rookh would never have been written
if the author's necessities had not compelled him to work.
'To keep himself at the oar, he contracted with the Long-
mans to supply a metrical romance on an Eastern subject,
which should contain at least as many lines as Scott's
Rokeby, an<l for which the publishers bound themselves to
[wy three thousand gixineas on delivery. The pncm w^.s
not published till May 1S17. Moore, as was his habit.
nade most laborious preparation, readir.g himself slowly
into familiarity ^^-ith Eastern scenery and manners. He
retired to a cottage in Derbyshire, near Lord iloira's library
at Doningtou Park, that he might work uninterruptedly,
safe from the distractions of Loudon society; and there,
" amid the snows of a Derbyshire winter " as he put it,
he patiently elaborated his voluptuous pictures of ilower-
scented valleys, gorgeous gardens, tents, and palaces,
and houris of ravishing beauty. The confidence of the
publishers was' fully justified. Moore's contemporaries
were dazzled and enchanted with Lalla Roohh. It was
indeed a wonderful tour de force. There was not a single
image or allusion in it that an ordinary Englishman could
understand mthout a foot-note. High testimonies were borne
to the correctness of the local colouring, and the usual stories
were circidated of Oriental natives who would not believe
that Moore had never travelled in the East. Moore was
less successful in realizing Oriental character than he was
in details of dress and vegetation. His fire-woj-shipper
is an Irish patriot betrayed by an informer, his Zelica a
piously niu'tured Catholic maiden brooding over unpardoned
sin, his ilokanna a melodramatic stage monster, — though
they are so thickly covered vv-ith Oriental trappings that
their identity is considerably disguised. Of the four tales
put into the mouth of Feramorz, the " Veiled Prophet " was
the least suited to Moore's Turkey-carpet treatment. We
can understand the enthusiasm with which Moore's Orien-
talism was received as " the best that we have had yet,"
and wo can honour the hoi;cst labour with whiui he
achieved this success ; but such artificial finery, as the poet
himself had the sense to suspect, could have only a temporary
reputation. He deliberately sacrificed the higher quaiitles
of poetry for accuracy of costume and soft melody of
rhyme and rhythm, and he had his reward. His ne.\t
Orientalism, the Loits of the Angels, published in 1822,
was hardly less popular than Lcdla Roohh. The artificiality
of the manufacture was shown by the ease with which,'
after a few editions, he changed his angels from Jews into
Turks, to evade a charge of impiety which was supposed
to impede the sale of the work. Lnmediately after tho
completion of Lalla Roohh Moore changed his residence
to Sloperton Cottage in Wiltshire, to be near Lord
Lansdowne and the library at Bowood, his next literary
project being a life of Sheridan. His plans were inter-
rupted by the consequences of the rascality of his deputy
.at Bermuda, which has been already mentioned. To
avoid arrest for the sum embezzled, Moore retired to the
Continent, and fixed his residence at Paris. He could not
return till November 1822, when the affair was com-
promised. His friends lamented that the attractions of
Paris occupied so much of his time, but, though his diary
contains almost daily records of visits to operas, fetes,
and fashionable entertainments, it shows also that he
was busier than he seemed. He wrote a goodly number
of squibs during his exile, besides composing the Loves of
the Angels and accumulating materials for his prose tale
of the Epicurean— !i fair amount of production consider-
ing his slow and painstaking habits of composition. His
alertness of mind, self-possession, and steadiness of purpose
enabled him to work as few men could in the midst of diver-
sions and distractions ; and, although he himself took a
brilliai.t }iart in conversation, we can see, from a compari-
son of his diary wth his published ^vritings, that he kept
his ears open for facts and iNatticisms which he afterwards
made his own. The darling of the drawing-room was as
much bee as butterfly. On his return to England he
resumed work steadily at his memoirs of Sheridan, ^vriting
Captain Rock as ajeu eCesprit by the way. The Sheridan
triumphantly despatched in the autumn of 1S25, Moore-'s
next important work was the Life of fiyrcn. 'The first
808
M O O — M 0 O
■volume of this was published early in 1 830, and tlie second
was ready by the eud of the same year. In 183] he com-
pleted a memoir of Lord Edward Fitzgerald, for which he
had been collecting materials for some time. Moore's
biographies call for no comment, except that they were
faithful and conscientious pieces of worJJ. He spent
much industry in the collection of characteristic anecdotes,
for which his position in society gave him exceptional
opportunity. His connexion with the biu-ning of Byron's
autobiography is too complicated a question to be dis-
cussed here. His own version of the ciixumstances is
given in his diary for May 1824.
It was a misfortune for the comfort of the last twenty
years of Moore's life that he aDowed himself to be drawn
into a project for writing the "History of Ireland" in
Lardne?s Cydopzdia. Scott and Mackintosh scribbled
off the companion volumes on Scotland and England with
very little trouble, but Moore had neither their historical
training nor their despatch in writing. Laborious con-
scientiousness and indecision are a fatal combination for
a man who undertakes a new kind of task late in life.
The history sat like a nightmare on Moore for fifteen
years, and after all was left unfinished on the melancholy
coKapse of his powers in 1845. From the time that he
bui dened himself with it Moore did very little else, beyond
a few occasional squibs and songs, the last Cashes of his
genius, and the Traoels of an Irish GenlUman in Search of
a lieligioii, although he had tempting offers of more
lucrative and, it might have been thought, more congenial
work. Moore's character had a deeper manliness and
sincerity than he often gets credit for ; and his tenacious
persistence in this his last task was probably due to an
honourable ambition to connect himself as a benefactor
with the history of his country, by opening the eyes of
the English people to the misgovernment of Ireland. It
was a misjudgment altogether ; the light irony of Captain
Rock was much more effective than the minute carefully-
weighed details of the historjf. Moore's last years were
harassed by the w&ikness and misconduct of his sens, and
by pecuniary embarrassments. i^Ji annual pension of
£300 was conferred upon him in 1833, and he had always
received large suras for his work ; but, while waiting for
the sinecure which never came, he had contracted an
unfortunate habit of drawing upon his pubUshers in
advance. After the death of his last child in 1845, Moore,
became a total wreck, but he lingered on till 26th Februaiy
185'2. The diary, which he seems to have kept chiefly
that it might be the means of making some provision for
his wife, and which contains so many touching expressions
of his affection for her, was edited by Lord -John liussell
with his letters and a fragment of autobio;jraphy in 1853-
56. The charge of vanity has often been brought against
this diary from the writer's industry in recording many of
the compliments paid him by distinguished personages and
public assemblies. It is only vanity that is annoyed by
the display of vanity in others. (w. M.)
MOOPt-HEN,' the name by which a bird, often called
"Water-hen and sometimes Gallinule, is most commoidy
known in England. An earlier name was Moat-hen, which
was appropriate in the days when a moat w?,s the ordinary
adjunct of most considerable houses in the country. It is
the GaUinula chloropus of ornithologists, and almost too
well known to need description. About the size of a small
Bantara-hen, but with the body much compressed (as is
usual with members of the Family liaHidx, to which it
belongs), its plumule above ia of a deep olive-brown, so
dark as to appear black at a short distance, and beneath
* Not to ba confiiuiidad with " Moor-cock " or " Moor-fowl." unmes
fonnerly in general U8« for tlio Ked Oroiue (voL xi. 2J1).
iron-grey, relieved by some white stripes on the flanks,'
with the lower tail-coverts of pure white, — these last being
very conspicuous as the bird svidms. A scarlet frontlet,
especially bright in the spring of the year, and a red garter
on the tibia of the male render him very showy. Though
often frequenting the neighbourhood of man, the iloor-
hen seems unable to overcome the inherent stealthy habits
of the Ho.Uidse, and hastens to hide itself on the least
alarm ; but under exceptional circumstances it may be
induced to feed, yet always suspiciously, with tanie ducks
and poultry. It appears to take wing with difficulty, and
may be often caught by an active dog; but, in reality, it
is capable of sustained flight, its longer excursions being
chiefly performed by night, when the peculiar call-note it
utters is frequently heard as the bird, itself invisible in
the darkness, passes overhead. The nest is a mass of
flags, reeds, or other aquatic plants, often aiTangcd with
much neatness, almost always near the water's edge, where a
clump of rushes is generally chosen ; but should a mill-dam,
sluice-gate, or boat-house afford a favourable site, advan-
tage will be taken of it, and not imfrequently the bough
of a tree at som-e height from the ground will furnish the
place for a cradle. The eggs, from seven to eleven in number,
resemble those of the Coot (vol. vi. p. 341), but are smaller,
lighter, and brighter in colour, 'sdth spots or blotches of
reddish-brown. In winter, when the inland watei-s are
frozen, the majority of Moor-hens betake theraiselyes to
the tidal rivers, and many must !e<tve the country entirely,
though a few seem always able to maintain their existence
however hard bo the frost. The common Moor-hen is
extensively spread throughout the Old Vt'orld, being found
also at the Cape of Good Hope, in India, and in Japan. In
America it is represented by a very closeiy-allied form, 0.
galeaia, so called from its rather larger frontal helm, and in
Australia by anotiier, G. tenelrosa, which generally wants
the white flank-markings. Both closely resemble G. ddor-
opus in general habits, as doea also the G. pyrrhorrlioa of
Madagascar, v/hich has the lower tail-coverts bull instead of
white. Celebes and Amboyna possess a smaller cognate
species, G. hsimaiopus, with red legs ; tropical Africa has
the smallest of all, G. angizlatn ; and some more that have
been rcooeiiized as distinct are also found in other more
or less jjsolated localities. One of the most remarkable of
these is the G. nesiotis of Tristan da Cunha,- which has
wholly lost the power of flight concomitantly with the
shortening of its wings and a considerable modification of
its external apparatus, as well as a strengthening of its peiiic
girdle and Icgs.^ A more extreme development in this
direction appears to be exhibited by the singiUar SabropCila
■wallacii of Jilolo,'' and to sone extent by tlie PareuJicsles
pacif.ati; of Samoa,^ but at present little is known of either.
Of other forms, such as the common GaUinula (En/tkra)
phoi/ticr.ra, and Gallirej; crislata of India, as well 8" <.)">
South-American species classed in the genus P'^phynops,
there is not room to speak ; but mention sho'ild be made
of the remarkable Australian genus Tr-.lony.<;, containing
three species,* which seem to bo af>ro terrestrial than
aouatic in their haunts and hablco
Allied to all these is the ^e-.oa Porphyria, including the
bird so named by claDsi'-al writers, and perhaps a dozeu
other species often 'bailed SrJtanas and Purple Water-
hens, for they a'l hi?e a plimii.ge of deep blue, — soma
becoming vio'oc, green, or black in parts, bat preserving
the white io'.ver tail-coverts, so generally characteristic
^ Pr'X. Hool. Society, 13i51, ;>. 280, pi. ixi.
' A Romewhat intermediate for.-u seems to be presented by thfi
Moor-hen of the islKud of St.D':fli.«>, to the north of -Madagoscjir (P:vCt
ZmI. Societ'j, 1887, p. lOSC), Lithorto undcscribed.
■* Op- cit., 1860, p. TdB, pi. cUiii.
' Op. eil., 1811, p. .ii, pi. ii.
• Ann. Aoi. History, aor. 3, xx. p. IDD,
M O O — M O R
809
of the group; ar.J flieir ueauty is cnlianced by tlieir scanct
bjil and hgs. Two, P. allmi of tbe Etliioj)iaii Region and
the South-American P. parva, are of small size. Of the
larger epecies, P. cxruteus is the "Porpliyrio" of the au-
cij'its, and inhabits certain localities on both sides of the
>Iediterranean, while the vest are widely dispersed -nnthin
ihe tropics, and even beyond them, as in Australia and
New Zealand. But this last country has produced a more
exaggerated form, Sotornis, -ndiich has an interesting and
perhaps vinique history. Fii-st described from a fossil skull
by Prof. Owen,^ and then thought to be extinct, an example
v.';!S soon after taken alive,^ the skin of which (with that
•of another procured like the first by Mr Walter Mantell)
7n.'i.y be seen in the British Museum. Other fossil remains
were from time to time noted by Prof. Owen ^; but it began
to be feared that the bii-d had ceased to exist,* until a third
example was taken about the year 1879, the skin and most
of the bones of which, after undergoing examination in
New Zealand by Dr Buller and Prof. T. .J. Parker,^ found
their way to the museum of Dresden, where Dr A. B. Meyer
■discovered the recent remains to be specifically distinct
from the fossil, and while keeping for the latter the name
Jf. mantdli gives the former that of iV. liocIisteUcn. AMiat
seems to have been a third species of Kotomia formerly
inliabited Lord Howe's Island, but is now extinct (see
BiKDS, vol. iii. p. 732, note). Whether the genus Apt-rmis,
of which Prof. Owen has described the remains from Nev/
Zealand, was most nearly allied to Notornis and PorjJnjno
-cannot here be decided. Prof. T. J. Parker {ioc. ck.) con-
siders it a "development by degeneration of an ocydromine
*3T® " (s^s Ocvdeome). (a. k. j
.MOOSE. See Deee, vol. vii. p. 2i.
jMOEADABAD. See JIubadabad.
MORAL PHILOSOPHY. See Ethics, vol. liii. p. 574.
MORATIN, Leandro Fernandez de (1760-1828),
Spanish dramatist and poet, was the son of N. F. Storatin
mentioned below, and was born at Madrid on 10th March
1760. His poetical and artistic tastes were early deve-
loped, but his father, keenly alive to the difficulties of the
li'erary calling, caused him to be apprenticed to a jeweller.
At the age of eighteen Moratin surprised liis friends by
wi:)rjng the second prize of the Academy for a heroic poem
-on the conquest of Granada, and two years aftcrv.-ards he
attracted still more general attention by a similar success
-of liis Leccion Poetv:a, a .satire upon the popular poets of
the day. Through Jovilianos he was now appointed secre-
tary to Cabarrus on his special mission to France in 1787,
s>.\-A daring his stay there he diligently improved his oppor-
i iiiities of becoming acquainted with the contemporary
'•'rench drama, and of cultivating the acquaintance of men
'A letters. Of the literary friendships he then formed the
/jost important was that with Goldoni ; indeed, Moratin
•'. much more correctly styled " the Spanish Goldoni " than
•' ihe Spanish Moliire." On his return to Spain Florida
Bianca prcientcd him to a sinecure benefice in Uio diocese
-of Burgos; and in 1790 his first play. El Viejo y la
Kiiia (The Old Husbaiu! and the Young Wife), a highly
finished but soniewliat dreary verse comedy iu t'iirco acts,
written in 1786, but delayed by objections of the actors.
' Pnc. Zodl. Sockl:^, 18-1-S, p. 7 ; Trails., iii. p. 336, pi. ivi.
= iVo&, 1850, pp. 2OO-2I5, pi. j;xL ; Tram., :v. pji. 69-74, pi.
3CXV.
- Thus lljo leg-bones aTid T\-hat appeared to be tTio stomum T\-ere
d^'wribed and figured bj* him {Trana., iv. jip. 12, 17, p!s. ii. iv.),
nnd the pelvis end another femur (vii. -pp. 369, S73, pis, .^lii. xliii. );
l>i-it the supi>osed sternum subsequently proved not to be that of
3Wom(5, and Professor Owen's attention being called to the fact he
rc.-tificd 'the error {Proc., 1SS2, p. 639) which he had pre\-iouBly
1>'!' ti "inclined to believe" (TVajw., viii. p. 120) he had made.
* Not7.'illist«ndinj the evidence, which it most be allowed pre-
sented some incongruities, otTered by Mr Mnckaj {Ibiot 1867, p. \H).
' TV/in* .V. ^eal. /.isf., :civ. pp. 238-:!l3.
was at length i.ioduced at tlie Teatro del Pnr.cipe. Its
success was only moderate. £/ Cii/e or La Comedia X^ieni.
on the other hand, given at the same theatre two years
afterwards, at once became deservedly popular, and had
considerable influence in modifying the public taste. It
is a short prose comedy in two acts, avowedly intended
to expose the follies and absurdities of the contemporary
dramatists — the school of Lope de A'ega run to seed — jvho
commanded the support of the masses ; and it is still read
with pleasure for the simple ingenuity of its plot, the live-
liness of its dialogue, and the easy grace of its style, wjiilc
to the student of literature it throws much useful light on
the contemporary state of the Spanish drama, and on the
refortoing aims of the author and his party. In the Same
year (1792) Florida Bianca was disgraced, but Moratin
at once found another patron in Godoy, who jjrovided him
with a pension and the means for foreign travel ; he accord-
ingly passed through France into England, where he began
the free and someiiMt incorrect translation of Havdct
which was printed in 17&8, but which has never been per-
formed. From England Ifae passed to the Low Countries,
Germany, Switzerland, ana Italy, and on his retm-n to the
Peninsula in 1796 he received-a lucrative post at the Foreign
Office. His next appearance in the drama did not take place
until 180.3, when El Baron was first pnblicly exhibited in
its present form. It successfully weathered a determined
attempt to damn it, and still keeps the stage. It was
followed in 1804 by La Mogigala (The Female 'E.jpo-
crite), of which imperfect manuscript copies had begun
to circulate as early as 1791. It was favourably received,
as on the whole it de.served to be, by a public which wa*
now at one with the author as to the canons of his art, and
an attempt to suppress it by means of the Inquisition on
alleged religious grounds (La Mogigata being an imitation,
a somewhat feeble one, of Moliere's Tariufe) was succass-
full}- frustrated. Sloratin's last and cro^vniug triumph in
the department of original comedy was achieved in 1803)
when El Si de las JTirias (A Girl's Yes) was perfonneA
night after night to crowded houses, ran through several
Spanish editions in a year, and was soon translated into
several foreign languages. In 1808, on the fall of the
Prince of the Peace, Moratin found it necessary to leave
Spain, but shortly afterwards he returned and consented
to accept the oflico of royal librarian under Joseph Bona-
paite — a false step;, which, as the event proved, permanently
alienated from him the sympathies of his country, and
compelled him to spend almost all the rest of his life in
exile. In 1812 his Esatela de los Maridos, a translation
and adaptation to the more dignified and stately Spanish
standard of Moliire's Ecole das Maris, was produced at
Madrid, and in 1814 El Medico a Palos (from Le Mededa
Malgre Lvi) at Barcelona. From 1814 to 1828 Moratin
lived in France, principally at Paris, and devoted himself
to the preparation of a learned work on the history of the
Spankh drama (Origmes del Teatro Espanot), which unfor-
tuni.iely stops short of the period of Lope de Tega. He
died at Paris on 21st June 1828.
An edition of I-.is Obras Dmmaticas y Liricas in tlu-ee voLs. was
published at Paris in 1825. The lyrical -ivorks, consisting of odes,
souneta, and ballads, are of comparatively little interest; tliey
reflect the influence of his father and of the Italian ContL The
best edition of the Obras is that published by the Spanish Academy
of History in four vols, at I.Iadrid in 1830-1S31 ; see also vol. iL
ci BU'Uokca dc Aulorcs jE'spaflu/cs (1816).
MORATIN, Nicolas Fernandez de (1737-1780),
Spanish poet, was descended from an old Biscayr.n family,
and was bom at Madrid in 1737. He was educated at
the Jesuit college in Calatayud, and afterwards studied
law at the univel-sity of Valladolid. He then received an
appointment in the service of Queen Elizabeth, the widow
ui Philip v., whi.'h enabled him 1 s see much of the, socieJy
'S-'.-L— 102
810
M 0 R — M 0 R
of leading c^tate.^mcn. ])Osra, and ineu of letters ; and
ultimately tie becaTne tlie leading spirit of the club of
literary men which frequented the Fonda de San Sebastian
and included Ayala, C'adahalso, Iriarte, Conti, and others.
In 1772 he left the court, and was called to the bar; four
years afterwards he succeeded A)ala in the chair of poetry
in the Imperial College. He died on 11th May 1780.
Moratic became at an eaily period of his life a convert to the
opinions of those who (such as Moutiano and others) were attempt-
ing to drive the native romantic diama from the Spanish stage, and
his fiist literary efforts were devoted to the cause of tlieatrical
rcforia. Il 1762 he published thiee small pamphlets entitled
Dcseru/nno at Tcatro EspnSiol (Tlio Trutli told about the Spanish
St-ige), ia which he severely criticized the old drama generally, and
particularly the still flourishing "auto sacramental" They were
so far successful that the exhibition of "autos saci-amentaies " was
prohibited by royal edict three yeais afterwards (June 1765). In
17C2 he also published a play entitled La Pctimctra (tho Petite-
Maitrestc, or Female Fribble), tlic earliest original Spanish comedy
formed avowedly on French models. It was preceded by a disserta-
tion in which Lope de Vega and Calderon are very unfavourably
ciiticized. Neither the Pctimctra, however, nor the Lucrccia, an
original tragedy still more stiictlj-in accordance with the conventions
of the French stage, ever obtained the honour of a public repre-
sentation. Two subsequent tragedies, Hormesinda (1770) and
Gtu^um cl Bvxno (1777), were exhibited with partial success. Ln
1761 Moratin pubUshed a collection of .=,hort pieces, chiefly Ij-rical,
under the title of Bl Pacta, and in 1765 a short didactic poem on
the chase (Diana o Arte de l<i Caza). His "epic canto on the
destraction of his ships by Cortes [Las Kares de Cortes Hc-itruidas),
written, but without success, for a prize offered by the Academy in
1777, was not published until after his death (17S5). It is justly
characterized by Ticknor as " the noblest poem of its class produced
in Spain during the 18th centurj- ; " it must be remembered, how-
ever, that the historical epic in Spain is cMefiy remarkable for its
mass. A voUlms of Obras Postumas, with a life, was pnhhshed
at Barcelona in 1821, and rejirinted at London in 1825. See also
j^ihliotua do Autorcs Espanolcs, vol. ii. (184G).
MOEAVIA (in German Mahken), a margraTiate and
crownlaiid in the Cisleithan part of the Austrian-Hungarian
empire, lies between 15° 5' and 18° 45' E. long., and 48°
50' and 50° 10' N. lat. Its superficial extent is about
t-'o80 square miles. Physically Moravia may be de-ccribed
as a mountainous plateau sloping from north to south, and
bordered on three sides by moimtain ranges of considerable
elevation. On the north it is separated from Austrian and
Prussian Silesia by the Sudetes, which attain a height of
4775 feet in the Altvater or Schneeberg, and sink gradually
towards the west, where the vaUey of the Oder forms a break
between the German mountains and the Carpathians. The
latter are the dividing range between Moravia and Hungary,
having here an average height of 3000 to 4000 feet. On
the west are the so-called Bohemian-Moravian mountains,
foi-ming the elevated east margin of Bohemia and descend-
ing in terraces, but without clearly-defined ridges, to the
river March. Branches of these diifereut ranges intersect
the whole country, maldng the sxu:face very irrcgiUar,
except towards the south, where it consists of fertile aud
c.-ctensive plains. Owing to this configuration of the soil
tlie climate varies more than might be expected in so small
an area, so that, while the vine and maize are cultivated
successfully in the southern plains, the weather in the
mountainous districts is somewhat rigorous. The mean
average temperature at Briirin is 48° Falu\ The harvest
amid the mountains is often four or five weeks later than
that in the south. Almost the whole of Moravia belongs
to the basin of the March or Moraia, from whieb it derives
its name, and wliich, after traversing the entire length of
the country in a course of 140 miles and receiving
numerous tributaries (Thaya, Hanna, <S:c.), enters the Dan-
ube at Pressljurg. T)ie Oder rises among the roouutaiiis
in tho north-east of Moravia, but soon turns to the north
and quits tho country. With the exception of a stretch of
the March none of the rivers are navigable. Moravia is
destitute of lakes, but contains numerous large ponds.
There are also several mincva! springs.
Nearly 97 per cent, of the soil of Moravia is pvoductiTOf
arable land occupying 53, gardens and meadows f>-i.
pasturage 0, and forests 26 per cent, of the total. It U
one of the chief corn-growing regions of the Austrian empire,
and also produces excellent hemp, flax, potatoes, vegetables,
and fruit. The following table shows the amount of the
chief crops in ISSl : —
■Wheat . . 451,480 qrs. Leguminous crops 27,8-50 cwt.
Rve . . . 1,242,180 ,, Beet (for sugar) ll,533,3i0 „
Barley . . 581,190 „ Flax .... 47,100 „
Oiits . . . 1,197,450 „ Hetnp. . . . 6,2C0 „
JIaizo . . 48,100 „■ Fniit .... 1,106,570 ..
Potatoes . 1,271, SSOcwt. Wine .... 2,869,460 galL
Large quantities of hay and other fodder, besides hops,
clover-seed, anise, fennel, <tc., are ai.so raised. The forests
on the slopes of the Sudetes produce abundance of excellent
timber. The live-stock of Moravia in 1880 consisted of
l-!2,858 horse-s, 677,807 cattle, 158,852 sheep, 20.5,976
swine, and 11(3,880 goats. The breed of sheep on the
Carpathians is of an improved quality, and tho horses bred
in the fertile plain of the Hanna are highly esteemed.
Gee=.e and poultry are also reared. In 1880 Moravia con-
t.oined 8.3,440 beehives, and the produce of wax aud honey
may be estimated at 3500 to 4000 c^vt3.
The mineral wealth of Moravia, consisting chiefiy of
coal and ii'on, is very considerable. In 18S1 the produce
included 392,6!,'5 tons of anthracite coal, 50,665 tons of
lignite, 5700 tons of iron-ore, 1713 tons of graphite, and
smaller quantities of alura, potter's clay, and roofing-slate.
The mines give em.ploymeut to 4500 persons, and the
annual value of the raw minerals produced is r.l'out
£370,000. The amount of raw and cast iron pro'luoed
by the ironworks and foundries in 1880 was 40,000 tors,
and the value about £320,000.
In point of industry Moravia belongs to the lOrciuo?!;
provinces of the empire. The principal manufacturi:s
are woollen, cotton, linen, and cast-iron goods, beet-sugAr,
leather, and brandy. Its wooUen cloths and flannels, tl.«
manufacture of which centres in Briinn, have long been
celebrated. Tho linen manufacture is decreasing in im-
portance as cotton manufactures develop. The quantity
of sugar made from beetroot is steadily increasing ; in
1880 about 600,000 cwts. of sugar were produced in r.fty-
sevca factories. About 10 per cent, of the total value of the
manui'actiu-es of Austria, representing an annual amount of
£13,000,000 to £15,000,000, falls to the share of Jlor.-ivji.
The trade of Moravia consists raairily in the exchanjo of
the various raw and manufactured materials above n-cn-
tioned for colonial produce, salt, and raw manufacturing
material. The lack of navigable rivers or canals is com-
pensated by good roads and an extensive railway .system.
The most important commercial towns are Briinn for manu-
factures and Olmiitz for live-stock.
In educational matters Moravia compares favourably
with most of the Austrian state;!. It contains 10 gj'mnasia,
10 rcal-g^Tiinasia, 13 real-schools, numerous schools for
special purposes, and nearly 2000 lower schools. The oM
university of Briinn is now represented b)- a technical
academy and a theological seminary. Of children of school-
going age 79 per* cent, attend school regularly. In 1S70
about 46 per cent, of tho Moravian recruits could Tvrite
their names, as compared with the exti-emes of 83i per
cent, in Lower Austria and 1^ per cent, in Dalmatia.
Fully 95 per cent, of the inhabitants are Pioman Catholics
under the ecclesiastical jurisdiction of tho archbishop of
Olmiitz and the bi.^hop of Briinn, while about 2 per cent,
are Jews, ond 3 per cent. Protestants.
Moravia sends 36 members to the Austrian reichstag,
9 of tliese representing the l.inded proprietors, 16 Ihij
towns and chaialeis of coni.n.cvce, and il llio pcasactiy,
M O R — M 0 R
Sll
Proviucial affairs are managed by the landtag, consisting
of the Roman Catholic archbishop and bishop, 30 repre-
sentatives of tlie landed gentry, 37 representatives of the
to^vns and chambers of commerce, and 31 representatives
of the country districts. There are six courts of justice
of the first insta,nce in Moravia, and one of the second
instance (at Eriinn), whence appeal lies to the supreme
court at Vienna. For military and judicial purposes
Moravia is united with Austrian Silesia.
Moravia belongs to the group of old Slavonic states
which have preserved their nationality while losing their
political independence. Upwards of 70 per cent, of the
inhabitants are Slavs, who are scarcely distinguishable
from their Bohemian neighbours. The differences in
dialect between the two countries are very slight, and are
being gradually lost in a common literary language. The
name of Czech, however, is usually reserved for the
Bohemians, while the Slavs of Moravia and West Hungary
are called Moravians and Slovaks. The zechs have lost
sight of iheir ancient tribal names, but the Moravians are
still divided into numerous secondary groups (Hovaks,
Hanaks, itc), differing sUghtly in costume and dialect.
The peasants usually wear a national costume. In the
south of Moravia are a few thousand Croats, still preserving
their manners and language after three centui'ies' separation
from their kinsmen in Croatia ; and in the north-e^.st are
numerous Poles. The Germans form about 26 per cent.
of the population, and are found mostly in the towns and
in the border districts. The Jews are the best educated
of the inhabitants, and in a few small towns form a full
half of the population. Their sympathies generally lie
ivith the Germans. In 1S80 the poj'ulation was 3,153,407,
showing an increase of 136,133 since 1800. Moravia is
one of the most densely- populated parts of Au-stria-Hungafy,
the proportion being 252 persons per square m.ile. About
12 per cent, of the births are illegitimate. The chief to\vns
are Briinn, the capital and industrial centre (S2,G60 irdia-
bitants), Olmiitz, a strong fortress defending the " Moravian
Gate" (20,176 inhabitants), Znaim, and Iglau.
History. ~Kt the earliest period of which we have any record
Moravia was occupieil by the Boii, the Celtic race which has per-
petuated its name in Bohemia. Afterwards it was ir.lialiited by the
Gerniauic Qiiadi, who accompanied the Vandals in theii- westw.ard
Diiffratioti ; and thoy were replaced in the 5th centiu^ by the Rugii
and Heruli. The latter tribes were succeeded about tbe year 550 A.n.
by the Lombards, and these in their turn were soon forced to retire
befoR' an overwhelming invasion of Slavs, who, on theh settlement
there, took the name ot Moravians (German, Mchmnen or JUahrcn)
from the river Morava. These new colonists became the pemianent
inhabitants of this disti-ict, and in spite of the hostility of the
Avars on the east founded the kingdom of Great itoravia, which
was considerably more extensive than the province now bearing
t^ie name. Towards the end of the Sth century lliey aided Charle-
m.agne in putting an end to the Avarldngdom, and were rewarded
by receiving part of it, corresponding to Kortli Hungary, as a fief
of the German emperor, who.'so supremacy they also acknowledged
more or less for their other possessions. After the death of
Charleraa^ie the Moi-avian princes took advantage of the dissen-
sions of his successors to enlarge their territories and assert their
iiid'^pcndcnce, and Rastislaus {circa 850) even fomied an alliance
irtth ine Bulgarians and the ByMutine emperor. The chief result
of the alliance v,-ith the latter w.as the conversion of the Jloravians
to Christianity by two Greek monks, Cyril and Methodius, des-
patched from Constantinople. Kastislaus finally fell into the
hands of Loxiis the German, who blinded him, and forced him
to end his days as a monk ; but his successor, Suatopluk ( ou. 890),
was equally vigorous, and extended the kingdom of Great iloraria
to the Oder on the west and the Gran on the east. At this period
there seemed a strong probability of the junction of the north-
western and soutli-eastcrn Slavs," and tho formation of a -great
Slavonic power to the oast of the German empire. This prospect,
however, was dissipated by tho invasions of the Mag>'ar hordes in
the 10th century, tlie brant of which was borne by lloravia. The
invaders were encouraged by the German monarchs and aided by
the dissensions and mismanagement of the successoiB of Suatopluk,
and in a short time completely suMued the eastern part of Great
iloi'avia. The name of iloi-avia was henceforth coiifiued to the
district to wl.i.-Ii it now applies. For about a century the posses,
siou of this nurchlaiid was disputed by Hungary, Pohmd, and
Bohemia, but in 1029 it was finally incnrporattd with Bohemia,
and so became an integral part of the German empire. Towards
the close of the 12th century Moravia was raised to the dignity of
a margraviate, but with the proviso that it should be held as a fief
of the crown of Bohemia. It henceforth shared the fortunes of
this country, and was Ubually assigned as an apanage to younger
membei-s of tlie Bohemian royal house. In HIO Jobst, margrave
of iloravia, was made emperor of Germany, but died a few months
after his election. In 152fi, on the death of Louis II. of Hungary,
iloravia came with tho rest of that prince's possessions into the
hands of the Austrian house. During tho Thirty Years' "War the
depopulation o( Moravia was so great that after the peace of West-
phalia the st.rtes-general published an edict giving every man
penn;=sion to take two wives, in order to "repeople the country."
After the Seven Years' War Moravia was united in one province
with the remnant of Silesia, but in 1849 it was made a separate
and independent crownland. The most noticeable feature of recent
MoiMvian histoij has been the active sympathy of its inhabitants
with the anti-Teutonic homo-rule igitatiouof the Bohemian Czechs
(see BoHE.\in).
/liiihoriliM.— Dudik, Ualireiu altgnnclne GeschictiU (Brfjnn, 1860.76); Tctny
Die .Karkgriifschaft Mdimn, topogmphixh, elaliUiicfi, tind hiilorlsch OMC/ifMert
(Brlnm, 1835-40); DElverf, BtUrdge itir Oachicitt der Ne^toeslallwm Miikrtm
lOT !,un Jahrhiindtrt (1807); Trampler, HiimaUkuridi dirr Hark iUhrcn
(Vienna, lb, 7); SialUUscM Jahrl-iicUr ot the Imperial SUtlsUcal ComtaiBsioa
CNienna). y p j, j
_ MORAVIAN BRETHREN, The, are a society of Chris-
tians whose history can be traced back to tho year 1457
and their origin found among the religious movements in
Bohemia which followed the martyrdom of John Huss by
the council of Constance. The beginniug.s of tho Bohemian
Bretliien (for that was their earlier name) are somewhat
obscure. The followers of Huss broke up into two factions,
one of which, the Calixtines, was willing to acknowledge
allegiance to Rome, provided the " compacts " of the council
of Basel permitting the Lord's Supper «ji utraque sjx'c'-'
were maintained, and in the end it became the uationr.l
church of Bohemia : the other, the Taborites, refused all
terms of reconciliation, and appealed to arms. Separate
from both these were many pious people who were content
to worship God in simple fasliion, in quiet meetings for
prayer and Scriptm-e-reading, like the Gottesfreunds of
Germany, and who called themselves Brethren. Boheiaian
historians have conclusively shown that the Brethren ret pre-
sent the religious kernel of the Hussite movement, and' do
not come either from tho German Waldeases or from the
Taborites. Before 1-157 many cf these quiet Christians
were Icnovn as the Brethren of Ch.elcic, and were tho
followers of Peter Chclcicky, a Bohemian, whose religious
influence, strongly Puritan in its character, seems to have
been inferior only to that of Huss. In thatye?,r the Calis-
tine leader, Rokyzana, wishing to protect them, permitted
his nephew Gregory to gather tliem together at KunewaU
near Senftenberg, and form them into a community. This
meeting was really the foundation of tho Brethren or Unitas
Fvatrum, and its founder Gregory announced that he and
his companions received and taught the rejection of oaths,
of tho military profeiision, of all official rank, titles, raid
endovvments, and of a hierarchy. They did not profess
commuDism, but they held that the rich should ^;ive of
their riches to the poor, and that all Clu'istians should live
po poarly a3 possible in the fashion of the apostolic com-l
mi'.-it'; &f- Jerusalem. At the synod ' of Lhota near
Reichenau, in l-ib7, they constituted themselves into a
cliurch separate fro-r. the CalLxtine or national church of
Bohemia. They appointed ministers of their own electic^n
and with the guidance of the " lot," and had an organi;;?.^
tion and discipline of their own ; at their hsad was a bishop,
who, it is said, received ordination froz: the Austrian
Waldenses, but apostolic succession among the BrctLren
is one of the most obscure parts of their history.
The constitution of tho society was revised at a second
synod held at Lhota under the direction of Luke of Prague,
who may ba regarded as their second founder. This re-
812
organization on.ihl.,] tiic woiefy to grow rapidlv Tn fl,.
.arher years of t),o 1 Gth centu./tho fnitastlLa no^
m congretjations ,n Bohemia and Moravia with 150 OOO
m,™bor.s,_and inch.ding Poland, en.braced thre , ov'fces
inwr;t^amonrthrRT' "' Germany awakened lively
nurest among the Brethren, and some unsuccessful at^
Km|,ts were made under the leadership of Au'us 1 1
■ n/te with the Lutheran Church HoOS }'iiL^lT\
.he Caivinist reformation reached Bo wft^'eBLl:"
P L^if J , , "^'''"" anti-Reformation, instigated bv
,.«., .», ,WrW i„ ,h, H,r™d cEbo? M.;/^ .'
Ss ': , i"' "tsr" s,:t .* -" - "*•'
,?s™r°ir' °" '" """^ •'»•'*•"■''' "'"la"
copate had been continued, and in 1735 Divid IVittl '
CimrcTThrnef \tf "'"' °^ 'he' '^Iwef ^^
+^^17 , settlement was not, however destined
The ernigrants at Herrnhut attended the paris^^ church S
Lc thelsdorf, and were sin>ply a Christian soc e y ^^-thfn
en>selvesasachurch mthin the church, or the BrethrTn's
™.wastherevivaUftn;^L:^-„'^-:^^-r^
M O K — H O R
woincn, are formalJv set ainrt s, jcoIvt« n
gieal. Special services ai-,-Vs«lorf>f- ,^'<'.^™'^'"P ■■lUur-
25th June, 6th Julv, 13th and 2Ist A> ^,J ' ^rlu o*''^' 1'"' »■"!
October, and 13th Novcu u' iL^t^^l' l^"" .?,=I?'ember, 31st
feet-washingand ti.e us- of tie lot in iw? T '"' ''"''*• '"" "'"
in marriages have fall™ into di use TWe of" tLlt™':"*'"- "<^
was abolished in 1818 ■'^"se 01 ttie lot m marriages
do^Hre:':s7or;,dL'r':Ld:r;?i^^''°r'r^' ="=-^' ^"' "«
and in the ,y,,,w„'n; A:,,,// „„ ' '" ""^Easter morning litanv,
by the s.vnod-'oasrgf •- 1) thlt'Sl'^ '^?"?;""« points" (settled
and praJtice m thoLt I J that Scripture is the only rule of faith
of GoT tel'it ,er %?« e ,'?^Tr'^>°' ^"?" "^'"«. (») the lo'
Jesus Christ ^1 n,',r , re^l Godhead and the real humanity of
before HimSorha:":'c'?fi'o:of''/° °°^'i '"' »" JustSoa
of the IIoi; GhostTnd the operatioL of H "''"'' '^^'''^ ^«tri"'=
as the fruit of the Spirit «f?refn f^^" ^^^i '' ' £"<"* '«"'':-^
another in Christ Jesus«) the 1/ ""'"P "^ ''^'i"'"" one with
and the resuireotion of% fe'dead un^liro',"f,?i "" "l""' '"-S'^^'
two divisons. (1) Boiiirlp^ ^„„„t ^ , '"•~^'"* <=mbiaees
mission, are carrS onttch prSe""! r^Ge,^""'"' ''°""'
there 13 a peculiar home mi«i,.V „.ii i\, r}^ Geruiau provii.ec
from 1729.^ Its object"' unlXian It^,' f 'T"™' ^""'■'' '^^<^'
spiritual life by means addTtional to t^L 'Vf^'^ "■"• ''°''t"
lished churches, and does not mlk" ^°'% ^^"'"^"^ ^^ "'^ "t^b-
principle of estabS?n^L V °"f '".n «'»* is conducted on the
vinces forty-seven boai'dri-school 'for bo :?."" 7 '^' ""™ P™"
Mith the Moravian Cluirel At .br.~?"i'^ S" Is net connected
are educated. ^"""^n- At these schools nearly 2500 pu;.i! >
(4) Foreign JIfissioiis.— The lloravi^r, n,„„i, •
zation by Ziuzendorf 1,»» 1,„1„ ,7°"\'™ Church since its reoigai.i.
The thi?d jub ee of missTon, w,'""TT "''^ ?^'-'"'^ >'"' oxcdtncc.
period began w th 1732 Xnt '^^'''•'"""1 i" 1882. The firet
&itschni?nn w re se'it t^ preadi ?o™th^°"'''' ^Tl^''^ ^^"-^
when it ended in 3 7S9 «,/T i ,, j "^Sroes of St Thomas;
occu,:,ying27ltatioi 'li'lssfth ^f ''I ^'f"'" ^"'l ^'^'^'^
^^1 7",. 7> , . "• ■'-v'iscants, and 76,646 converts.
ISro. I't nowcontansfourcr.." T' '"^'T-''""''' '" '^''°^'^'
legal sanction. «"gregations, and in ISSO obtained
(d) The Leper MUsion was begun in 1829 in <!r,„ii, at ■ -, '
earned on there till 1S67 when the Pno-l ki: r- ^'"''■^- """^
acl,ai>lai„ to do the work UrKu™™";'''' "^
established in 1867, a, d formallv t^k^^ T I'l! ^7;"^'™ "^
encc of the Unity hiTssi ^ ^" ^^ ""' '''^'""' "■^"-
'•" -'""«'« ius a cnurcn.
diocesan. Thev ore annointcl I.v ti,,. "'""""■, b"t they are not
SteUisiics. —
r/«: r/ira Uonic Provinces.
Bishops . . J A
Ticsbytcrs and Deacons 291
Communicants . J8 871
j Foreign and Bolvemian
I Bishops
I Jlissioiiailes .
Temale Agents ',
Native Jlinistei-s and
Assistants .
Native Agcnis
Communicants
Missions.
167
110
35
1,524
2 vols London, 1825 ; Bost, llisl. je ftw « ',l-. ?7 '^"'' '"'""' *'»««,,
of ra°f ^f"['^^;r^BS;; itlTe7tb^^ ^ri
ici 1. TV. Lit bciiinr liou'vh-d P P b,. ♦!.„ J . ,
Loirc-Liforicurc, E. Iv tlA ■ 111. ■,(••' \^'l'''<^"^ ''^
. -.y iij.u ci iiie-ot-A ilatne, X. by Cot«3
M O R — M O 11
813
du Xord, and V,'. by I'mHti,re. Its chief town, Vannes,
is 248 miles west-south-west of Paris in a direct line and
310 by rail. From the ilontagnes Ifoires on the northern
fronfier the western portion of Jforbilian slopes southward
towards Finistire, watered by the Quimperle, the Blavet
mth its affluent the >Scorff, and the Aiiray; the eastern
portion, on the other hand, dips towards the south-east in the
direction of the couiiij of the Oust and its feeders, which
fall into the Vilaine. Though the Hontagnes Noires con-
tain the highest point (975 feet) in the department, the most
stiiking orographic feature of Morbihan is tlie dreary, tree-
less, streamless tract of moorland and marsh known as the
Landes of Lauvaux, which extends (west-north-west to east-
south-east) with a width of from 1 to 3 miles for a distance
of 31 miles between the valley of the Ciaie and that of the
Arz (affluents of the Oust). A striking contrast to this
district is afforded by the various inlets of the sea, whose
shores are clothed with vegetation of exceptional richness,
large fig-trees, rose-laurels, and aloes growing as if in
Algeria. The coast- line is exceedingly irregular : the
mouth of the Yilaino (the longest river of the department),
the peninsula of Euis, the great gulf of Morbihan (Inner
Sea), from which the department takes its name, and" the
mouth of the Auray, the long Quiberon peninsula attached
to the mainland by the narrow isthmus of Fort Penthifevre,
the deep-brancliing estuary of Etel, the mouths of the
Blavet and the Scoi-ff uniting to form the port of Lorient,
and, finally, on the borders of Finistfere the mouth of the
Laita, follow each other in rapid succession. Off the coast
lie the islandsof Groix,Bellfe-isle, Houat,andHoedik. Vessels
drawing 13 feet can ascend the Vilaine as far as Redon ;
the Blavet is canalized throughout its course through the
department ; and the Oust, as part of the canal from Nantes
to Brest, forms a great waterway by Eedon, Josselin, Rohan,
and Pontivy. The climate of Morbihan is characterized
by great moisture and mildness, due to the influence of the
Gulf Stream.
Of the 2625 square miles fonniug the department, nearly, one
hair is occupied by moonj {landes), arable soil formiug little more
than a tliii-d part of the whole, meadows a tenth, and woodlands
a efteenth. The horses number 36,000, horned eattle 285,000,
sheep 92,000, pigs 60,000, goats 6000, and beehives 76,000. In
1882 the agricultural produce comprised 3,751,680 bushels of rye
and 1,544,170 bushels of wheat; and considerable quantities of
hu^ckwheat, oats, potatoes, pease and beans, chestnuts, beetroot,
hemp, colza, and flax are grown. A little wiue also is made, but
tile usual liquor of the district is cider (inajuifactured to the extent
of 11 to l3 million gallons per annum). The sea-ware gathered
aioug the coast helps greatly to improve the soil. Outside of
Loiieut there is little industrial activity in Morbilian, though
canvas, leather, preserved foods, paper, and chemical products
derived from the sea are all manuf:*£tured. Salt marshes give
employment to 400 hands, and yield on an average 9502 tons of
salt; and slate, kaolin, iron-ore, and granite are also worked. The
catching and curing of sardines aiid the breeding of oysters form
the business of many of the inhabitants of the coast, who also fish
f6r anchovies, lobsters, kc., for tinning. There are 154 miles of
railway in the department, and it was intended (1883) that the line
from Nantes to Brest sliould have branches from Auray to St Brieuc
and to Quiberon, aud from Questcmbert to Ploermel. Morbilian
is divided into four arrondissements, — Vannes, Lorient, Ploermel,
and Pontivy — 37 cantons, and 249 commuues. The population in
1881 was 621,614. • '
Few departments contain so many localities interesting for their
historical associatione. Besides the megalithie monuments of
C.iRX.\c (2S00 inhabitants) (.q.v.) and of Locmariaqucr (20i)0),
may be mentioned — Sarzeau (5720) with its castle of Sueinio, one
of tho ancient dukes of Brittany ; Josselin (2710) with the tomb
of Olivier de Clisson, constable of France, and of his second wife
Marguerite de Rohan ; the castle of the Kohans, and in the neighbour-
hood a column in memory of the "Combat of tlie Thirty ;" Guenu-ne
(1570) and the chateau of the Rohan Guemenc family ; Le Palais
(4685), the chief phicc in Belle-isle, containing the chateau of
i'ouquet (Louis XlV.'s superintendent of fiiiance) and the hospital
erected by his wife. Quiberon (2380) is associated uith the disiister
of the French emigres ; Hennebont (60:'n) has a magnificent lailway
viaduct over ihe Blavet, and La Kocho Bernard (1230) a suspension
bridge over the Vilaine, C46 feet long and 108 feet above spring
tides.
MORDAUXT, CH.UiLEs. See Peterbokough, ILmL op,
MORDVLNLVXS, more correctly Moedva or Mordvs,
are a people numbering about one million, of Finnish
origin, belonging to the Ural-iUtaic family, who inhabit
the middle Volga provinces of Russia and spread in small
detached communities to the south and east of these.
Their settlement in the basin of tho Volga is of high
antiquity. One of the two great branches into which
tliey are divided, the Aorses (now Erzya), is mentioned
by Ptolemy as dwelling between the Baltic Sea and the
Ural mountains, whilst the Aorses of A.sia occupied at
the same time the countrj' to tho north-east of the Caspian
between the Volga and the Jaxartes. Thuir king is said
to have come with 200,000 horsemen to aid llithradates
in his wars. Strabo mentions also the Aorses as iidiabit-
ants of the country between the Don, the Caspian Se.i,
and the Caucasus. The name of Mordvs is mentioned
for the first time by Jordanes, and they were known
imder the same name to the Russian annalist Nestor. The
Russians made raids on the Mordvs in the 12th century,
and after tho fall of Kasan they rapidly invaded and
coloniied their abodes. The Mordvs now occupy the
Russia!) provinces of Simbirsk, Penza, Samara, and Nijni-
Novgorod, as well as those of Saratofi' and Tamboff. But
their villages are dispersed among those of the Russians,
and they constitute only 10 to 12 per cent, of the popu-
lation in the four fir->t-named provinces, and from 5 to
6 per cent, in the last two. They are unequally distri-
buted over this area in ethnographical islands, and con-
stitute as much as 23 to H per cent, of the population of
several districts of the governments of Tamboff, Simbirsk,
Samara, and Saratoff, and only 2 or 3 per cent, in other
districts of the same provinces. A small number of Mordvs
are found also in the provinces of Ufa, Orenbui-g, Astrakhan,
and even in Siberia as far east as the river Tom. They
are divided into two great branches, the Erzya and the
Moksha, differing in their ethnological features and in their
language. The southern branch, or the Moksha, have a
darker skin and darker eyes and hair than the northern.
A third branch, the ICaratays, is due to mixture with
Tatars, whilst a fourth branch, mentioned by several
authors, is, according to Mainoff, but a local name for
pure Mordvs. Theu- language is considered by M. AMqvist
as the third branch of the Western Finnish family, the two
other branches being the Laponian and the Baltic Fimiish,
Avhich last embodies now the lang-aages of the Karelians,
the Tavastes, the Wotes, the Wespes, the Esthcs, and the
Lives. The Mordvs are for the most part completely
Russified,— even the Mokshas who consider themselves as
the only pure Mordvs, — yet they have well maintained
their ethnological features, and can be easily distinguished
even when living completely as Russians. They have
neai'ly quite forgotten their own language, ordy a few
women remembering it among the Mokshas ; but they
have maintained a good deal of their old national dress,
especially the women, whose profusely embroidered skirts,
original hah-dress, large earrings which sometimes are
merely hare-tails, and numeroas necklaces covering all the
chest and consisting of all possible ornaments easily dis-
tinguish them from Russian women. They have mostly
dark hair, but blue eyes, generally small and rather narrow.
The cephalic inde.x of the Mordvs is very near to that of
the Films. They are brachyeephalous, or sub-brachycepha-
lous, and a few are mesaticephalous. They are finely biult,
rather tall and strong, and broad-chested. Their chief occu-
pation is agriciUture ; they work harder and (in the basin
of the Moksha) arc more prosperous than their Russian
neighbours. Thtir caoacities as carpenters were well
814
M O R — H O R
knoim in Okl Russia, and Ivan tlio Terrible used them to
liuild bridges and clear forests during bis advance on ICasan.
At present th:-y manufacture in their villages great
quantities of wooden ware of various sorts. They are also
"Tcat masters of apiculture, and the commonwealth of bees
often appears in their poetry and religious beliefs. All
explores are unanimous in recognizing their honesty,
morality, and sympathetic character ; it is noticed also
that thoy have remarkable lingiustic capacities, and learn
with great cose not only BAis.sian but also several Finnish
and Turkish dialects. Nearly all are Christians ; they
received baptism in the reign of Elizabeth ; the Koncon-
formists have recently made many fervent proselytes among
them. But they still preserve very much of their own
rich mythology, which they have adapted to a certain ex-
tent to the Christian religion. They have preserved also,
especially the less Kussitied Moksha, the practice of kid-
napping brides, with the usual battles between the party
of the bridegroom and that of the family of the liride. The
worship of trees, water (especially of the v,'ater-diTinity
which favours marriage), the sun or Shkay, who is the chief
divinity, the moon, the thunder, and the frost, and that
devoted to the home-divinity Kardaz-serko can be seen in
full force among them ; and a small stone altar or flat
stone covering a .^mall pit to receive the blood of slaughtered
animals can be found in very many houses. Their burial-
customs are of a quite pagan character. On the fortieth
day after the death of a kinsman the dead is not only
supposed to return home but a member of his household,
dressed in his dress, plays his part, and, coming from the
grave, speaks in his name. The practice of animal sacrifice
is still deep rooted among the Mokshas, who continue to
drink the warm blood of immolated animals.
Tho Mordvs have always liad a great attraction for Russian
incpiirei's ; Strahlenberg, Georgi, Pallas, and especially Lepekliin
have wi-itten about them. Melnikoff has published in several
Ku.'isian periodicals interesting sketches of tlieir religious beliefs.
A gieat number of smaller sketches have appeared in periodicals ;
th:-:-;; are enumerated by BiainolT in the Izvcsiia of the Russian Geo-
graphic-al Society for 1877. Entrusted by the Geograpliical Society
\vitti ihe study of this race, Slainoff has recently made extensive
anthroixdogical measurements and studies of their customs and
Gommon4aw. The results are published, but not yet in full, in
tiie Izfcstia of the Russian Geogi-aphical Society for 1878, and in
«ie peiiodicals Slovo for 1879, and Old and Kcw Jimsia ioT 1878.
They were to appear in full in tho Memoirs of the Society.
MORE, HAi^NAH (1745-1833), who was born at Staple-
ton near Bristol in 1745, may be said to have made three
reputations jn tho com-se of her long life : first, as a clever
verse-writer and witty converser in the circle of Johnson,
Reynolds, and Garrick ; next, as an aniinated writer on
mosal and religious subjects on the Puritanic side ; and
lastly, as a practical philanthropist. She was the youngest
but one of the five daughters of Jacob More, a scion of a
landed Norfolk family, who taught a school at Stapleton
in Gloucestershire. Tho sisters established a boarding-
school at Bristol in 1767. Hannah's first literary efforts
were pastoral plays, suitable for young ladies to act,
published in 1773 under the title of 'A Search after
Happiness. Jletastasio was one of her literary models;
on his opera of Reyulus she based a drama, The Injiexihle
Capiit-e, published in 1774. An annuity from a wealthy
admirer set the young lady free for literary pursuits.
Some verses on Garriek's Lear led to an acquaintance ;
Miss More was taken up by the gi-eat female Jfa;cenas,
Mrs Montague ; and her unaffected enthusiasm, simplicity,
vivacity, and wit won the hearts of the whole Johnson
set, the great lexicographer himself being especially fasci-
nated. Miss ilore was petted, complimented, and en-
couraged to write. Her ballad, Eldred of the liower. was
praised and quoted by the liighest living authorities ;
and she wrote for Oarrick the tragedy Percy, which was
acted with great success in 1777. Another drama, The
Fatal Falsehood, produced in 1779 after Garriek's death,
was less successful. In these dramas .she borrows from
Shakespeare situation, imagery, and phraseology with
greater freedom than modern criticism would tolerate ;
but they are written with great vigour, freshness, and
effect. Rer Sacred Dramas appeared in 17S2. These
and the sprightly octosyllabic poems Bas-BUu and Flmio
(17SG) mark her gradual transition to more serious views
of life, which were fully expressed in prose in her ThoughU
on the Manners of the Great (17SS), and An Estimate of the
Rcliijion of the Fashionable World (1790). She had never
been overpowered by the flattering reception given her in
fashionable society ; she had received its attentions ^vith
misgivings and reservations, never touching cards, keeping
Sunday strictly, and preferring company where she could
have serious conversation ; and finally, soon after Garriek's
death, she set herself against theatre-going luider any
pretence. There is great uniformity of tone and topic in
her ethical books and tracts : — Strictures on Female Educa-
tion (1799), Hints toviards forminy the Character of a
Young Princess (1805), Goelchs in Search of a Wife (only
nominally a story, 1809), Practical Piety {\8llj. Chris-
tian Morals (1813), Character of St Paid (1815), Moral
Sketches (1818). 'The tone is uniformly animated; the
WTiting fresh and vivacious ; her favourite subjects the
minor immoralities, the thoughtless self-indulgences and
infirmities which are rather indirectly than dii-ectly harmful.
She was a rapid "\\Titer, and her work is consequently
discursive and formless ; but there was an originality and
force in her way of putting commonplace sober sense and
piety that fully accoimts for her extraordinary popularity.
An interesting epi.'<ode in her Uteraiy life was her three
years' labour in writing spirited rhymes and prose tales in
the Cheap Repository .series (1795-1798) to counteract the
doctrines of Tom Paine and the influence of the French
Revolution. Two millions of these rapid and telling
sketches were circulated in one year, teaching the poor in
rhetoric of most ingenious homeliness to rely upon the
virtues of content, sobriety, humility, industry, reverence
for the British constitution, hatred of the French, trust
in God and in the kindness of the gentry. Perhaps the
noblest testimony to Hannah Jlore's sterling worth was
her indefatigable philanthropic work — her long-continued
exertions to improve the condition of the children in the
benighted districts in the neighbourhood of her country
residences at Cowslip Green and Barley Wood. ■ Sh*
limited her aims strictly, as a good churchwoman ant
anti-Revolutionist, to teaching them to read good books
and trying to raise their moral tone ; but no philanthropist
ever laboured at greater self-sacrifice or with purer motives.
In her serene old age, philanthropists from all parts of the
world made jiilgrimages to see the bright and amiable old
lady, and she retained all her faculties till within two
years of her death, dying at Clifton on 7th September
1833, at the mature age of eighty-seven.
MORE, Hexey (1614-1687), one of the most remark-
able and interesting of the "Cambridge Platonists," was
born at Grantham in Lincolnshire in the year 1G14. His
father was " Alexander More, Esq., a gentleman of fair
estate and fortune," highly sjioken of by his son, who
attributes to his father his own poetical tastes and generous
love of learning from his early youth. Both his father
and mother, ho further tells us, were " earnest followers of
Calvin," but he himself " could never swallow that hard
doctrine." As soon as ho went to Eton he gave himselS
up to what he considered a more genial and encouiMging
train of religious thought. From his boyhood in the Eton
playing-fields he was a philosophical and religious dreamer,
and he describes his moods of religious reverie in a very
MORE
815
interesting manr.cr.' Hi3 comraunings and ct.-'li/.ii,.- ]:ave
no morbid taint ; they are the natural carriage ol ;, st rangely
gifted spirit. " From the beginning all things in a manner
came flowing to him," and his mind, according to his o\Yn
Eayins, "was enlightonrd with a sense of the noblest
theories in the morning of his days." In 1G31 he went
to Cambridge, and was admitted at Christ's College abont
the time Milton was leaving it. Ho immersed himself
" over head and ears in the study of pliilosoi'ihy," and fe!!
for a time into a sort of scepticism, from which, hov.evcr,
lie was delivered by a study of the "Platonic writers."
He wa-s fascinated especially by NeoPlatonism, and this
fascination never left him. The Tueotof/ia Gennanica also
exerted a gi-eat and permanent influence over him. He
entered upon a course of spiritual self-discipUne which
made all his previous studies seem of comparatively no
value ; and gradually light as well as peace came to him.
He got "into a most jorous and lucid state of mind,"
which hs described in a Greek epigram, as he had formerly
described his state of mental and spiritual darkness in the
same manner. He took his bachelor's degree in 1635, his
master's degree in 1639, and immediately afterwards was
chosen fellow of his ccUege. In this position he may be
said to have rcinaiucd all hi? life. JIany offers of prefer-
ment were made to him, but he refused them all, with one
exception. Fifteen years after the Restoration, he accepted
a prebend in Gloucester catliedral, but only to resign it in
favour of his friend Dr. Edward Fowler, afterwards the
well-known bishop of Gloucester. He had no ambition,
and steadily declined all attempts to draw him towards
public life. He would not even accept the mastership of
his college, to which, it is understood, he would have been
preferred in 16.54, when Cudworth was appointed. He
drew many young men of a refined and thoughtful tum
of mind around him, but among all his pupils the most
interesting was a young lady of noble family, a " heroine
pupil," as his biographer (Ward) says, " of an extraordinary
nature." This lady is supposed to have been a sister of
f-nt-d Finch, afterwards earl of Nottingham, a wcll-kno\vn
statesman of the Eestoratiou. She afterwards became
Lady Conway, and at her country seat at Eagley in
Warwickshire More continued at intervals to spend " a
considerable part of his time." She and her hu-sband both
greatly appreciated him, and amidst the woods of this
pleasant retreat he composed several of his books. There
is reason to think that the spiritual enthusiasm of Lady
Conway was a considerable factor in some of More's
speculations, none the less that she at length passed from
his religious pupilage into the ranks of the Quakers.
Susceptible to all the excited impulses of her time, this
lady became the friend not only of More and Penn but of
Earon van Helmont and Valentine Greatrakes, mystical
thaumaturgists who played a considerable part amid the
teeming enthusiasms of the 17th century. Ragley became
a centre not only of devotion but of wonder-working spirit-
ualism.- " Many happy days," More says, he spent in this
"paradise," and its fantastic mysticism had more allure-
ments for him than he himself realized. His genius suficred
in consequence, and the play of rationality which distin-
guishes his earlier is much less conspicuous in his later
works. He was a voluminous writer both in verse and
prose, and the mere list of his works would occupy more
space than we can give to it. JIany of his -productions
are now unreadable ; but the Divine Dialogues, published
in 1G6S, may be still read with pleasure. It is animated
""■" sometimes even brilliant, with less prolixity and
.-li^ressiou than his other productions, while it has also
J 'Trefiitii Generiilissima " prefi.ted to his Ojim Omnia, 1679.
- The j>ln:c and its religions man-cls are glauced at in the roaiance
the advantage for modem readers that it cotidenses his
general view cf philosophy or.d icii^non. Most of his
characteristic principles may in fact be gathered from it.
The year in which he composed the Divine Diidogwa
may be said to mark the highest point of his intellectual
activity. His Manual of Metay/hysics and elaborate treat-
ises en Jacob Boehme and Spinoza were subsequent to
thia : but the elasticity and freshness of his philosophical
geuius are Icc-s buoyant in these efforts, ai.d the prophetico-
mystical elements which were a weakness in bis luental
constitution from the first grew as his years advanced.
He represents mors than any other member of the school
the mystical and theosophic side of the Cambridge move-
ment. Us lofty rationality, the rationality of. which ho
himself had spdkcn earlier in noble language, at length
evaporates in him in intellectual rccrie and dreams. The
Neo-Platonic extravagances which lay hidden in the school
from the first came in his writings to a head, and mergul
in pure phantasy, — a set of fa\oui-ite ideas which not
merely guided but dominated the reason. Withal Henr\
More can nsver be spoken of save as a spiritual genius and
significant figure in the history of Britisli philosophy, less
robust and manly and in so:ne respects less learned than
Cudworth but more interesting and fertile in thought, and
more sweet, singular, and ge:ual in character. From youth
to age he describes himself as gifted witli a most happy and
buoyant temper. The presence of nature filled lum with
rapture ; ha wished he could be always S!<4 dio. " AValk-
ing abroad after his studies his sallies towards nature
would bo often inexpressibly ravishing, beyond what he
could convey to others." His own thoughts were to him
a never-ending source of pleasurable excitement. His
mind moved with great rapidity and at a lofty elevation,
so that, as he .says, he seemed " all the while to be in the
air." This mystical glow and elevation were the chief
features of his mind and character, a certain transport and
radiancy of thought which carried him beyond the common
life without raising him to any false or artificial height,
for his humility and charity were not less conspicuous than
his piety. The last ten years of his life are without any
special record, and he died on the morning of 1st September
1687, and was buried in the cLapel of the college te loved
so well, where witliin less than a year his friend Cudworth
was laid beside him.
Before his death Jtoro issued complete editions of his works, "iis
Opera Thcoloffica iu 1675, and his Opera Philosaphica in IGTa.
Tlie chief authorities for his life are Ward's Life, 1710 ; the "Pre-
iitio Generalissima " prefixed to his Opera Omnia, 1679 ; and also
a general account of th« manner and sco^ie of his writings iu an
Apology published in 1661. The collection of his Philosophical
Poems, 1647, in which he has "compared his chief speculations
and experiences," sliould also be consulted. An elaborate analy-
sis of his life and works is given in Principal Tulloch's PmHoimI
Theology, vol. ii., 1874. (J- T.)
MORE, Thomas (1478-1535), lord chancellor, and one
of the most illustrious Englishmen of his century, was
born in Milk Street iu the City of London, 7th February
1478. He received the rudiments of education at St
Anthony's School in Threadneedle Street, at that time
under Nicolas Holt licld to be the best in the city. He
was early placed in the household of Cardinal Morton,
archbishop of Canterbury. Admission to the cardinal's
family was esteemed a high privilege, and was sought as
a school of manners and as an introduction to the world
by the sons of the best families in the kingdom. Young
Thomas More obtained admission through the-influence of
his father. Sir Thomas, then a rising barrister and after-
wards a justice of the Court of King's Bench. The usual
prognostication of future distinction is attributed in the
case of More to Cardinal Morton, " who would often tell
the nobles sitting at table with him, where young Thomas
waited on him. whosoever liveth to trie it shall see tJiit
816
U ORE
cliild prove a notaUc and r.iic nia:i." ' At dio j<ropcr age
young Mere vas scut to Oxfoi'il, wborc In; U said vs-uely
to have liad Culet, Crocyn, ami Liiiacro for his tutors.-
';VU Jlorc liimsclf says is tliat ho haJ Linaci-e for hh niat-lor
in Creek. Learning Greek wai not the matter of couisc
which it has since beco'nic. Greek was not as yet part of
iho arts curriculum, ai^il to learn it voluntarily was ill
looked upon by the authorities. Those who did so -were
suspected of an inclination towards novel and dangerous
modes of thinking, then rife on the Continent and slowly
finding their way to England. Morc's father, who intended
Ills son to make a career in his own profession, took the
alarm ; he removed him from the university without a
degree, and entered him at Xew Inn to commence at
once the study of the law. The young man had been
kept in a state of humiliating dei)cndence in money
matters, having had no allowance made him, and having
had to apply to his father even for a pair of nevir shoes
when the old were worn out. This sy^tem was pursued
by his parents not from niggardliness but on principle ;
and Thomas More in later years often spoke with appro-
bation of this severe discipline, as having been a means of
keeping him from the vulgar dissipations in which his
fellow-students indulged. After completing a two-years'
course in New Inn, an lun of Chancery, More was admitted
in February HDO at Lincoln's Inn, an Inn of Court. "At
that time the Inns of Court and Chancery presented the
discipline of a well-constituted university, and, through
professors under the name of readers and exercises under
the name of mootings, law was systematically taught"
(Campbell). In his professional studies More early dis-
tinguished Iiimself, so that he was appointed reader-in-law
in Furnival's Inn ; but he would not relinquish the studies
which, had attracted "him in O.xford. We find him deli-
vering a lecture to audiences of " all the chief learned of
the city of London." ^ The subject he chose was a com-
promise between theology and the humanities, being St
Augustine's De Civitate. In this lecture More sought less
to expound the theology of his author than to set forth
the philosophical and historical contents of the treatise.
The lecture-room was a church, St Lawrence Jewry, placed
at his disposal by Grocyn, the rector.
Somewhere about this period of Jlore'a life two things
happened which gave in opposite directions the dOtermin-
ing impulse to his future career. More's was one of those
highly susceptible natures which take more readily and
more eagerly than common minds the impress^ of that
which they cncoimter on their iirst contact with men.
Two principal forms of thought and feeling were at this
date in coniiict, rather unconscious than declared, on Eng-
lish soil. Under the denomination of the "old learning,"
the sentiment of the Jliddla Ages and the idea of church
authority was established and in full possession of the
religious houses, the universities, and the learned profes-
sions. The foe that was advancing in the opjiosito direc-
tion, though without the conscience of a hostile pui-pose,
was the new power of human reason animated with the
revived sentiment of classicism. In More's mind both
these hostile inlluences found a congenial liome. Each
had its turn of supremacy, and in his early years it seemed
as if the humanistic influence would gain the final victory.
About the age of twenty he was seized with a violent
access of devotional rapture. He took a disgust to the
world and its- occupations, and experienced a longing to
give himself over to an ascetic life. He took a lodging
near the Charterhouse, and subjected himself to the disci-
pline of a Carthusian monk. lie wore a sharp shirt of
hair next hi.-3 skin, scourged himself every Friday and
Llh bv P. r..
Life by B. E.
^ Rppcr, L'/c,
! other fasting Jay-, lay upon the bare ground ^^ ith a log
! under his head, and allowed himself but four or live hours'
sleep. This access of the ascetic malady lasted but a short
time, and More recovered to all outward appearance liis
balance of mind. But he never entirely emaucipatcl
liimsclf from the sentiment of devotion, though in l-'ter
life it e.vliibited itself in a more rational form. Eveis
when he was chancellor he would take part in church
services, walking in their processions with a surplice.
This, howevei', was at a later time. For the moment the
balance of his faculties seemed to be restored .by a revival
of the antagonistic sentiment of humanism which he had
imbibed from the Oxford circle of friends, and specially
from Erasmus. The dates as regards More's early life
are uncertain, and we can only say tliat it is possible that
the acquaintance with Erasmus might have begun during-
Erasmus's first visit to England in 1499. Tradition has
diamati.zed their first meeting into the story given by
Cresacre More,' — that the two happened to sit oppo.«ito
each other at the lord mayor's table, that they got into
an argimient during dinner, and that, in mutual astonish-
ment at each other's wit and readir.ess, Erasmus e.v-
claimed, "Aut tu es Morns, aut nuUu.s," and the other
replied, "Aut tu es Erasmus, aut dLabolus I " iiejcct-
ing this legend, which bears the stamp of fiction upon its
face, we have certain evidence of acquaintance between
the two men in a letter of Erasmus with the date "Oxfo/d,
"29th October 1499." If we must admit the correctness of
the date of J!p. 1 4 in the collection of Erasmus's EpisioU;
we should have to assume that their acquaintance had
begun as early as 1497. Ten years More's senior, wkI
master of the accomplibhments which More was ainbit'\6us
to acquire, Erasmus could not fail to exercise a powiii-ful
influence over the brilliant young Englishman. More's
ingenuous demeanour, quick intelligence, and winning
manners fascinated Erasmu.s from the first, and acquaiiil-
ance rapidly ripened into warm attachment. This contai t
with. the prince of letters revived in More the spirit o^ the
" new learning," and he returned with ardour to the stmly
of Greek, which had been begun at Oxford. The humanistic
influence was sufiieiently strong to save him from wrecking
his life in monkish mortification, and even to keep him
for a time on the side of the party of progress. He ac-
quired no inconsiderable facility in the Greek languag';,
from which he made and published some translations.
His Latin style, though wanting the inimitable ease of
Erasmus and often ofi'endiug against idiom, is yet in
copiousness and proprietj' much above thex)rdinary Latin
of the English scholars of his time.
!More's attention to the new studies was always subor-
dinate to his resolution to rise in his profession, in which
he was stimulated by his father's example. As early as
1.502 he was appointed under-sheriff of the city of London,
an oflice then judicial, and of considerable dignity. He
first attracted imblic attention by his conduct in the
parliament of 1504, by his daring opposition to the king's
demand for money. Henry Vll. was entitled, according
to feudal laws, to a grant on occasion of his daughters
marriage. But ho came to the House of Commons for a
much larger sum than he intciuled to give with his daughter.
The members, unwilling as ihcy were to vote the money,
were afraid to otlend the king, till the silence was bi-oken
bj' More, whose speech is raid to have moved the House
to reduce the subsidy of three-fifteenths which the Govern-
ment had demanded" to £30,000. One of the chamberlain,'*
went and told his master that he had been thwarted by a
beardless boy. Henry never forgave the audacity ; but,
for the moment, the only revenge ho could take vras ni>oii
^ Lifi, p. 93.
MORE
817
More's father, whom upon some pretext he threw into the
Tower, and he only released him upon payment of a fine
of £100. Thomas More even found it advisable to with-
draw from public life into obscurity. During this period
of retirement the old dilemma recurred. One while he
devoted himself, to the sciences, "perfecting himself in
music, arithmetic, geometry, and astronomy, learning the
French tongue, and recreating his tired spirits on the viol,"'
or translating epigrams from the Greek anthology ; another
while resolving to take priest's orders.
From dreams of clerical celibacy he was roused by
making acquaintance with the family of John Colt of
New Hall, in Essex. The "honest and sweet conversation"
of the daughters attracted him, and though his inclination
led him to prefer the second he married the eldest, not
liking to put the affront upon her of passing her over in
favoiu' of her younger sister. The death of the old king
in 1507 restored him to the practice of his profession, and
to that public career for which his abilities specially fitted
him. From this time there was scarce a cause of import-
ance in which he was not engaged. His professional in-
come amounted to w£400 a year, equal to £4000 in present
money, and, "considering the relative profits of the law
and the value of money, probably indicated as high a
ptation as £10,000 at the present day" (Campbell). It
•was not long before he attracted the attention of the young
iking and of Wolsey. The Latin verses which he pre-
sented to Henry on the occasion of his coronation did not
deserve particular notice amid the crowd of congratulatory
odes. But the spirit with which he pleaded before the
Star Chamber in a case of the Crown v. the Pope recom-
mended him to the royal favour, and marked him out for
employment. More obtained in this case judgment against
the crown. Henry, who was present in person at the trial,
had the good sense not to resent the defeat, bu* took the
counsel to whose advocacy it was due into his service. In
!1514 More was made master of the requests, knighted, and
ewom a member of the privy council. He was repeatedly
employed on embassies to the Low Countries, and was for a
long time stationed at Calais as agent in the shifty nego-
tiations carried on by Wolsey with the court of France.
In 1519 he was compelled to resign his post of under-
sheriff to the city and his private practice at the bar.
In 1521 he was appointed treasurer of the exchequer, and
in the parliament of 1523 he was elected speaker. The
choice of this officer rested nominally with the House
itself, but in practice was always dictated by the court.
Sir Thomas More was pitched upon by the court on this
occasion in order that his popularity with the Commons
might be employed to carry the money grant for which
Wolsey asked. To the great disappointment of the coiu't
More remained firm to the popular cause, and it was greatly
owing to his influence that its demands were resisted.
From this occurrence may be dated the jealousy which
the cardinal began to exhibit towards More. Wolsey
made an attempt to get him out of the way by sending
•him as ambassador to Spain. More defeated the design
by a personal appeal to the king, alleging that the climate
Tfould be fatal to his health. Henry, who saw through
the artifice, and was already looking round for a more
popular successor to Wolsey, made the gracious answer
that he would employ More otherwise. In 1525 More
was appointed chancellor of the duchy of Lancaster, and
no pains were spared to attach him to the court. The
king frequently sent for him into his closet, and discoursed
,with him on astronomy, geometry, and points of divinity.
This growing favour, by which many men would have
been carried away, did not impose upon More. He dis-
16—30
' Roper, H/e '
couraged the king's advances, showeil rdnclanco to "go t«i
the palace, and seemed constrained when th'.To. Then
the king began to come himself to Morc'-i linusc at Chelsen,'
and would dine with him without jupWous notice. Koih.t
mentions one of these \-isit3, when t)ie king after dinntr
walked in the garden by the space of an hour, holding
his arm round More's neck. Eoper afterwards conjrat*;
lated his father-in-law on the distinguished honour flhirli
had been shown him. "I thank oiu- Lord," was the reply,
" I find his grace my very good lord indeed ; and I believe
he doth as singularly favour me as any subject AviHiin this
realm. Howbeit, son Eoper, I may tell thee I li.ivo no
cause to be proud thereof, foi if my head would wi:s hiui
a castle in France, it should not fail to go." As a last
resource More tried the expedient of silence, di^seiubliiig
his wit and afiecting to be dull. This had the dc.-ireil
effect so far that he was less often sent for. But it did
not alter the royal policy, and in 1529, when a succe.ssor
had to be found for Wolsey, More was raised to the
chancellorship. The selection was justified 1>y More's high
reputation, but it was also significant of the modification
which the policy of the court was then undergoing. It
was a concession to the rising popular purty, to which ^t
was supposed that More's poUtics inclined him. The
public favour with which his appointment had been
received was justified by his conduct as judge in thf
Court of Chancery. Having heard causes in the forenoon
between eight and eleven, after dinner he sat again to
receive petitions. The meaner the suppliant was the
more affably he would speak to him, and the more speedily
he would despatch his case. In this respect he formed a
great contrast to his predecessor, whose arrears he soon
cleared off. One morning being told by the oflScer that
there was not another caiise before the court, he ordered
the fact to bo entered on record, as it had never hajipened
before. He not only refused all gifts, such as had been
usual, himself, but took measures to prevent any of hit
connexions from interfering with the coiu'se of justice.
One of his sons-in-law. Heron, having a suit in the chan-
cellor's court, and refusing to agree to any reasonable
accommodation, because the judge "was the mast affec-
tionate father to his children that ever was in the world,"
More thereupon made a decree against him
Unfortvmately for Sir Thomas Jfore^ a lord chancellor
is not merely a judge, but has high political functions to
perform. In raising More to that eminent position, the
king had not merely considered his professional distinction
but had coimted upon his avowed liberal and reforming
tendencies. In the Utopia, which, though written earlier,
More had allowed to be printed as late as 1516, he had
spoken against the vices of power and declared for indif-
ference of religious creed ^vith a breadth of philosophical
view of which there is no other example in any English-
man of that age. At the same time, as he coiUd not be
suspected of any sympathy with Lutheran or Wickliffite
heretics, he might fairly be regarded as qualified to lead
the party which aimed at reform in state and church
wdthin the limits of Catholic orthodoxy. But in the king^
mind the public questions of reform were entirely sunk in
the personal one of the divorce. The divorce was a point
upon which Sir Thomas would not yield. And, as he saw
that the marriage with Anne Boleyn was determined upon,
he petitioned the king to be allowed to resign the great
seal, alleging failing health. With much reluctance, the
royal permission was given and the resignation accepted,
10th May 1532, with many gracious expressions of good
will on the part of the king. The promise held out of
future botmty was never fulfilled, and More left office, as
he had entered it, a poor man. His necessitous condition
was so notorious that the clergy in convocation voted him
818
MOKE
a present of £5000. This he peremptorily refused, either
for himself or for his family, declaring that he '"had rather
sea it all cast into the Thames." Yet the whole of his
income after resigning office did not exceed £100 a year.
Hitherto he had maintained a large establishment, not
on the princely scale of Wolsey, but in the patriarchal
fashion of having all his sons-in-law, \vith their families,
under his roof. When he resigned the chancellorship he
called his children and grandchildren together to explain
his reduced circumstances. " If we wish to live together,"
said he, " you mu.st be content to be contributories together.
But my counsel is that we fall not to the lowest fare first :
we will not, therefore, descend to Oxford fare, nor to the
fare of New Inn, but we will begin with Lincoln's Inn
diet, where many right worshipful men of great accouut
and good years do live full well ; which if we find our-
selves the first year not able to maintain, then we will in
the next year come down to Oxford fare, where many
great learned and ancient fathers and doctors are continu-
ally conversant ; which if our purses stretch not to main-
tain neither, then may we after, with bag and wallet, go
a-begging together, hoping that for pity some good folks
will give us their charity."
More was now able, as he writes to Erasmus, to retuiii
to the life which had always been his ambition, when, free-
from business and public aifairs, he might give himself up
to his favourite studies and to the practices of his devotion.
Of the Chelsea interior Erasmus has drawn a charming
picture, which may vie with Holbein's celebrated canvas,
The Household of Sir Thomas More.
" ^lore lias built, near Loudon, upon the Thames, a modest yet
commodious mansion. There he lives surrounded by his numerous
femily, including his \rife, his son, and his son's wife, his three
daughters and their husbands, mth eleven grandchildi-en. There
is not any man living so affectionate to his children as he, and he
loveth his old wife as if she were a girl of fifteen. Such is the
excellence of his disposition that whatsoever happeneth that could
not be helped, he is as cheerful aud as well pleased as though the
best thing possible had been done. In More's house, you would
say that Plato's Academy was revived again, only, whereas in the
Academy the discussions turned upon geometry and the power of
numbers, the house at Chelsea is a veritable school of Christian
religion. In it is none, man or woman, but readeth or studieth
the liberal arts, yet is their chief care of piety. There is never any
seen idle ; the head of the house governs it not by a lofty carriage
and oft rebukes, but by gentleness and amiable manners. Every
member is busy in his place, performing his duty with alacrity ;
nor is sober mirth wanting." ^
But Mors was too conspicuous to be long allowed to
enjoy the happiness of a retired life. A special invitation
was sent him by the king to attend the coronation of
Anne Boleyn, accompanied with the gracious offer of X20 to
buy a new suit for the occasion ! More refused to attend,
and from that moment was marked out for vengeance.
A first attempt made to bring him within the meshes
of the law only recoiled with shame upon the head of the
accusers. They were maladroit enough to attack him on
his least vulnerable side, snnunoning him before the privy
council to answer to a charge of receiving bribes in the
administration of justice. One ParnoU was put forward
to complain of a decree pronounced against him in favour
of the contending party Vaughan, who he said had pre-
sented a gilt cup to the chancellor. More stated that ho had
rexieived a cup as a New Year's gift. Lord Wiltsliire, the
queen's father, exultingly cried out, " So, did I not tcU
you, my lords, that you would find this matter true ? "
"But, my lords," continued iloro, "having pledged Mrs.
Vaughan in the wine wherewith my butler had filled the
cup, I restored the cup to her." Two other charges of a
like nature were refuted as triumphantly. But the very
futility of the accusations must hnvo betrayed to More
» Aj). iiSjjipp.
the bitter determination of his enemies to compa.t; hia
destruction. Foiled in their first ill-dii-ected attem))t,
they were compelled to have recourse to that tremendous
engine of regal t}Tanny, the law of treason. A bill was
brought into parliament to attaint Elizabeth Barton, a
nun, who was said to have held treasonable language.
Barton turned out afterwards to have been an impostor,
but she hail duped More, who now lived in a superstitious
atmosphere of convents and churches, and he had given
his countenance to her supernatural pretensions. Hi3
name, with that of Fisher, was accordingly included in
the bill as an accomplice. When he came before the
council, it was at once apparent that the charge of treason
could not be sustained, and the efforts of the court agent 3
were directed to draw from More some approbation of !' ■•
king's marriage. But to this neither cajolery nor thre.. , ;
could move hira. The preposterous charge was urged ihi.^
it was by his advice that the king had committed himseit
in his book against Luther to an assertion of the pope's
authority, whereby the title of " Defender of the Faith "hr.d
been gained, but in reality a sword put into the popc'j
hand to fight against him. More was able to reply that
he had warned the king that this very thing might happen,
that upon some breach of amity between the crown of
England and the pope Henry's too pronounced assertion
of the papal authority might be turned against himself,
'■therefore it were best that place be amended, and his
authority more slenderly touched." "Nay," replied the
king, " that it shall not ; we are .so much bound to the see
of Kome that we cannot do too much honour unto it.
Whatsoever impediment be to the contrary, we will set
forth that authority to the utmost ; for we have received
from that see our crown imperial," "which," added More,
" till his grace with his own mouth so told mo, I nevr-r
heard before." Anything more defiant and exasperating
than this coidd not well have been said. But it could not
be laid hold of, and the charge of treason being too
ridiculous to be proceeded with, More's name was struck
out of the bill. When his daughter brought him the
news. More calmly said, "I' faith, Meg, quod differtur,
non aufertur : that which is postponed is not dropt." At
another time, having asked his daughter how the court
went, and how Queen Anne did, he received for answer,
" Never better; there is nothing else but dancing and sport-
ing." To this More answered, "Alas, Meg, it pitieth ma
to remember unto what misery, poor soul, she will shortly
come ; these dances of hers will prove such dances that
she will spurn om- heads off like footballs ; but, it will not be
long ere her head will dance the like dance."^ So the .speech
runs in the Life by More's great-grandson ; but in the only
trustworthy record, the life by his son-in-law Roper, More's
reply ends with the words, " she will shortly come." In thi.s,
as in other instances, the later statement has the appear-
ance of having been aa imaginative extension of the earlier.
In 1534 the .\ct of Supremacy was passed, and the
oath ordered to be tendered. More was sent for to
Lambeth, where he offered to swear to the succession, but
steadily refu-ied the oath of supremacy as against his con-
science. Thereupon ho was given in charge to the abbot
of V/estminster, and, pei-sisting in his refusal, was four
days afterwards oonuuitted to the Tower. After a closa
and even cruel confinement (he was denied the use of pen
and ink) of more than a year, he was brought to trial before
a special commission and a packed jury. Even so Jlore
woiUd have been acquitted, when at the last moment
Rich, the sohcitor-general, quitted the bar and presented
himself as a witness for the crown. Being sworn, he
detailed a confidential conversation he had had with the
' Cresacie More. .p. 231.
M O R — M O E
819
prisoner in the Tower. He affinned that, having himself
admitted in the course of this conversation '' that there
were things which no parliament could do, — e.g., no parlia-
ment could make a law that God should not be God," Sir
Thomas had replied, " No more could the parliament make
the king supreme head of the church," By this act of perjury
a verdict of "guilty" was procured from the jury. The execu-
tion of the sentence followed within the week, on 7th July
1535. The head was fixed upon London Bridge. The ven-
geance of Henry was not satisfied by this judicial murder
of his friend and servant ; he enforced the confiscation of
what small property More had left, expelled Lady More
from the house at Chelsea, and even set aside assignments
which had been legally executed by More, who foresaw
what would happen before the commission of tne alleged
treason. More's property was settled on Princess Elizabeth,
afterwards queen, who kept possession of it till her death.
At his death Sir Thomas More was in the fifty-eighth
year of his age. He was twice married, biit had children
only by his first wife. His eldest daughter Margaret,
married to William Roper, is one of the foi-eraost women
ib the annals of the country for her virtues, high intelli-
gence, and various accomplishments. She read Latin and
Gieek, was a proficient in music, and in the sciences, so
f.j as they were then accessible. Her devotion to her
father is historical ; she gave him not only the tender
afTection of a daughter but the high-minded sympathy of
a soul gi"eat as his own.
It is unfortunate for More's reputation that ho has been adopted
AS a champion of a party and a cause which is arrayed in hostility
to the liberties and constitution of hia country. Apart from the
partisan use which is made of his name, we must rank him among
the noblest minds of England, as one who became the victim of a
tyrant whose policy he disapproved and whose servile instruments
ho despised. If his language towards the tyrant is often more
servile than became a freeman, wo must remember th.at such was
the court style of tlie period, and that we must not consti'ue liter-
ally phrases of compliment. It is, however, impossible to deny
thatJIore's policy in later life did not bear out the more liberal
convictions of his earlier yeai-s. His views and feelings contracted
under the combined influences of his professional practice and of
public employment la the Utopia, published in 1516, he not only
denounced the ordinary vices of power, but evinced an enlightenment
of sentiment which went far beyond the most statesmanlike ideas
to be found among his contemporaries, pronouncing not merely for
toleration but rising even to the philosophical conception of the
indifference of religious creed. It was to this superiority of view,
and not merely to the satire on the administration of Henry VII.,
that we must ascribe the popularity of the work in the 16th cen-
tury. For, as a romance, the UUipia has little interest either of
incident or of character. It does not, as has been said, anticipate
the economical doctrines of Adam Smith, and much of it is fanciful
without bei.ng either witty or ingenious. Mackintosh says of it :
" It intimates a variety of doctrines, and exhibits a multiplicity
ff projects, which the writer regards with almost every possible
degree of approbation and shade ol assent, from the frontiers of
serious and entire belief, through gradations of descending plausi-
bijity, where the lowest are scarcely more than exercises of ingenuity,
and to which some wild paradoxes are appended, either as a vehicle,
or as an easy means, if necessary, of disavowing the serious inten-
tion of the whole of this Platonic fiction."
Tlie Epistola ad Dorpium at a later date exhibits More em-
phatically on the side of the new learning. It contains a vindi-
cation of the study of Greek, and of the desirability of printing
the text of the Gi-eek Testament,— views which at th»t date required
an enlightened understanding to enter into, and wliich were con-
demned by the party to which More afterwards attached hiiasclf.
At the most, he can be doubtfully exculpated from the charge of
havuig tortured men and children for heresy. It is admitted by
himself that he inflicted punishment for religious opinion. Erasmus
only ventures to say in his friend's defence "that while he was
chancellor no m.an was pnt to death for these pestilent opinions,
♦whUe so many suffered death in Franca and the Low Countries."
T'lfr «^' "f.^''^"^, Mo" "M wrltt« by his son-in-law Roper about the
Ha £. A^ ', F- ","'" f"'^"<''i I" MS. dnrlng tlio reign of Elizabeth,
and handed about in copies, many of which were earefcs«ly made. It was not
lilJlf/ii^f-iT'?*'!! '^l°'„'"y' *^^ ''"'« o' ^'^- Reprints were made by
rf,™ 0. 1''), >y Leivts 0729, 1731X and by Singer (1817, 182-.>). Roper's life &
S?i?';„„„ ^"'?1>"5^,'''"';i""°S'^'''"«»- M0re-8Li/«lnMs!(Harleian
.i. A ??''>'". "L'',''"' ^y ^'eolM Harpsllcld, was also written in MaiVs rei'm
All liat u 8l:iterial in this MS. is taken from Roper. Aether a°on^.?Jzf?.;
written !n 1W9, printed In Wordtworth'a EecUtiaitteaS Bl-^rapJiy, U. 43-186, is
chiefly complied from Roper and Harpslield. The preface is signed R B.
Stapletoo (IVftj Thcmse, a. ret gestm S. Thoma apoBioU, S. TJiomje arcMepiieopi
CantuaHentU, Thcma MoH, Douay, 15SS, Ck)logne, 1612, and the Vita Thomm
Mori (separately), Gratz, 1639) translates Roper, interweaving what material he
could find scattered through More's works and letters and the notices of him
in the writings of his contemporaries. Cresacre More, great-grandson of 8Ir.
Thomas, compiled a new life abont the year 1627. It was printed without date,
but, according to the editor. Hunter, in 1631. The title of this edition is— Tis
Life of Sir Thos. More, Lord High CkancelUntr of England, 4to, s. 1. eta., and with
new title-page, 1642, 1726, 1823. This life U cited by the subsequent biographers
as an independent authority. But it is almost entirely borrowed from Roper
and Stapleton. The additions made have sometimes the appearance of rhetorical
ampliflcations of Roper's simple statements. At other times they are decor-
ative miracles. The whole is couched Id that strain of devotional exaggeration
in which the lives of the saints are usnally composed. The author seems to
imply that he had received euperaatural communications fi-om the spirit of his
ancestor. Already, only eighty years after More's execution, hagiography bad
taken possession of the facts, and was transmuting them into an edifyinglegend.
Cresacre More's Life cannot be alleged as evidence for anv facts wtiich are not
otherAvise vouched. It has been remarked by Hunter that More's life and worlts
have been all along manipulated for political poiToscs, and In the interest of
ths holy see. In Mar^^s reign, and in the tide of (Catholic reaction. Roper and
H.irpsfield wrote lives of him ; Ellis Heywood deJicated his 11 Moro to Cardinal
Pole, and Tottell reprinted the folio of his English worics. Staplcton prepared
his Trcs Thomas in 1588, when the recovery of England to the see of Rome was
looked for by the Spanish invasion. In 1509, when there was a prospect of a
disputed succession, the anonymous Life by B. R. w.is composed : and soon after
Charles had alUed himself with a Catholic, the Life by Cresacre More issued from
the press. Hunter might have added that Stspleton was being reprinted at
Gratz at the time when the conversion of England was expected from James II.
The later Uvea of Sir Thomas More have been numerous, but the only one which
has any critical value is that by G. T. Rudhart Thomas Moms, aus den Qucllen
bearbeitet, Nuremberg, 1829. Other lives are by J. Hoddesdon, London, 1662,
1662 ; by Cayley, 2 vols., London, 1808 ; by Mackintosh, Lardner's Cab. Cyclop.,
London, 1831, 1844 ; and in More's Works, London, 1845 : by Lord Campbell in
Lives of the Chancellors, vol. i., l&4S-oO ; by D. Nisard in Rei^aissance ct Sefomu ;
by Baumstark, Freiburg, 1879. A biographical study on Mote's Latin poems
is PUlomorus by J. H. Marsden, 2d ed., London, 1S78.
More's writings are numerous, and a complete bibliogTaphy of them would
occupy several columns. His English Works were collected and published in
one vol. folio by RastaU, London, 1530, and reprinted by Tottell, London, 1557.
His Latin ITor/cs were also separately collected in one vol., Eaasl, 1563 ; Louvain,
1560; and, riiost complete, "I-'rankfort and Lelnslc, 1689. The t^topia has had
numerous editions, the first is Louv., 1516. There ate two English translations
of the Vtcpia, byR. Robynson, London, 1551, 1556, 1624, and by Gilb. Burnet,
1688. Tho Latin poems, Frogymnasmala, appeared in 1518, 1520, 1563. This
last ed'tion cont.iins the Utopia and other prose Latin pieces. (M. P.)
MOREAIt, HioKsippE, a minor lyric poet of disputed
but considerable talent, was born at Paris on the 9th April
1810, and died in the hospital of La CharitS on the ]Oth
December 1838. Lq his early youth his parents, who were
very ill-off, migrated to Provins, where the mother went
into service and the father took the post of usher in a
public school. Both died in the same refuge for the desti-"
tute which afterwards received their son. Heg^sippe was
fairly educated and was apprenticed to a printer, but he
preferred the work (in France usually paid most miserably)
of " maltre d'lStudes " in a school. He went to Pai-is before
1830, and appears to have practised both his occupations
there, though for the most part he cither adopted by choice
or was driven by ill-fortune to adopt the singular life of
alternate hardship and cheap dissipation which is dignified
in France by the name of Bohemianism. In Moreau's casa
there is no doubt that tho hardships exceeded the dissipa-
tion. He was habitually houseless, and is said to have
exposed himself to the dangers of a cholera hospital in
the great epidemic of 1832 simply to obtain shelter and
food. Then he revisited Provins and published a kind of
satirical serial called Diojene. Some years of this life
entirely ruined his health, and it was OLjy just before his
death that he succeeded in getting his collected poems
published, selling the copyright for £i sterling and eighty
copies of the book. It was received not unfavo'orably,
but, as has happened in other cases, the author's death,
which happened soon in the circumstances mentioned, was
required to excite an interest which was proportionately
excessive. Moreau's work, like tliat of many other young
poets, has a strong note of imitation, his model being
esp(;cially B6ranger ; and his character, both moral and
literary, is not improved bj' obvious.affectation in political,
religious, and social matters. But some of his poems, such
as La Voulne and the charming La Fermicre, have great
sweetness, and he had a faculty of ■writing both in prose
and poetry which seems to show that with better fortune,
or, to speai honestly, with more intelligence and more per-
severance he might easily have saved himself from the
miserable destitution which was his Igt.
820
MO R — M O R
MOREAIT, Jean Victoe (1763-1813), the greatest
general of the French republic after Napoleon and Heche,
was born at Mbrlaix in Brittany in 1763. His father
was an " avocat " in good practice, and instead of allowing
him to enter the army, as he wished, insisted on his
studying law at the university of Rennes. Young Morcau
showed no inclination for law, but revelled in the freedom
of a student's life. Instead of taking his degree he con-
tinued to live with the students as their hero and leader. In
that capacity he became a person of political importance,
and in the troubles of 1787 formed the law students into
a sort of army, which he commanded as their provost. In
1789 he became yet more imijortant, and commanded the
students in the daily affrays which took place at Rennes
between the young noblesse, who protested against the mode
of election to the states-general, and the populace. Though
he had hardly weight enough to be chosen a deputy, he
waa elected one of the committee of correspondence with
the deputies at Paris. He was thus able to foUow the
coiu-se of events in the early days of the Revolution, and
was early impressed ■nath the conviction that no compromise
with the court was possible, and a republic the only re-
source. These opinions estranged him from his father,
who belonged to the party of Breton independence and
preferred Brittany to France. At last, in 1792, at the
call for volunteers he organized a battalion, and was at
once elected its commandant. With it he served under
Dumouriez, and in 1793 the good order of his battalion,
and his own martial character a;id republican principles
.■■.ecured his promotion as general of brigade. Carnot, who
had an eye for the true qualities of a general, promoted
him to be general of division in 1794, and gave him com-
mand of the right wing of the army v/hich, under Pichegru,
was destined to drive the English and Austrians out of Flau-
' ders by separating the Austrians from the English. This wing
was then to cover the occupation of Holland by the main
army under Pichegru. These operations established his
military fame, aad in 1 795 he waa given the command of the
army of the Rhine and the Moselle, with which he crossed
the Rhine and advanced into Germany. He was at first
completely successful, and won several victories, but at last
had to execute before the archduke Charles a retreat v/hich
only increased his fame, as he managed to bring back with
J:im more than 5000 prisoners. In 1797 he again crossed
the Rhine, but his operations Were checked by the con-
clusion of the preliminaries ot Leoben between Bonaparte
and the Austrians. It was at this time he found out the
traitorous correspondence between his old comi-ade and
commander Pichegru and tho prince de Cond^, which he
foolishly concealed, and naturally has ever since been sus-
pected of at least partial' complicity. After Fructidor the
Directory ceased to employ his service, until the absence of
Bonaparte and the advance of Suwaroff made it necfessary
to have some great general in It?.ly. Yet it was only as
chief of the staff that he served under Scherer and Joubert,
nnd led bac.k the French army after the latter's death at
KoW. When Bonaparte returned from Egj'pt he found
Moreau at Paris, greatly dissatisfied with the Directory both
fs a general and as a republican, and obtained his assistance
in tho coup d'etat of Brumaire, when Moreau commanded
the force which occupied the Luxembourg. In reward,
the first consul again gave him command of the army of the
Rhine, with which he fought hia last great campaign, that
of Hohenlinden, when his success was duo ratlier to the
splendid military qualities of his generals and their troops,
and his ovm tactical genius, than to any insjiiration of
victory. On his return to Paris ho married Mdlle. Hullot,
an ambitious woman, who gained a complete a.sccndency
over him, and with the enormous fortime acquired during
his campaigns he purchased a luxurious hotel in Paris and
also Barras's country-seat of Grosbois. His wife exercised an
evil influence over him, and collected around her all who were
discontented with the aggrandizement of Napoleon. This
" club Moreau " frightoicd Napoleon, and encouraged the
royalists ; but Morcau, though not unwilling to become a
military dictator to restore the republic, would not intrigue
for the restoration of Louis XVIII. All this was well
known to Napoleon, who sfeized the conspirators. Moreau
he treated with real leniency, and permitted to retire first
to Spain, and then to America. Here the general lived
in great content for seven years, when his wife, who could
not allow him to rest, made him enter into negotiations
with Bernadotte, his old comrade, who was now crown-
prince of Sweden. At his suggestion Moreau entered the
service of the czar Alexander ; and with Bernadotte
he planned the campaign of 1813. Fortunately for his
fame as a patriot he did not live to invade France, but
was mortally wounded while talking to the czar at the
battle of Dresden on 27th August 1813, and died on 2d
September. His wife received a pension from the czar,
and was given the rank of mar^chale by Louis XVIII.
Moreau's fame as a general stands very high, and from his mar-
vellous coolness in conducting retreats he has been called the general
of retreats. His combinations were splendid, and his temper al.vays
unruffled wheu most closely pressed ; but he laclied the sudden spirit
of seizing a victory which distinguished Napoleon in his early cam-
paigns, iloreau was a sincere republican, though his own father was
guillotined in the Terror ; and the army of the Khine was the hot-
bed of republicanism, as that of Italy was the great support of a
military tyranny. As a man, he was little given to personal ambi-
tion till his marriage, and would probably not only have seiTcd
Napoleon well but moderated his tendency to absolutism by his
very e.xistence, had not his wife i-uined any such hope by involving
him in intrigues. He was fortunate in the moment of his death,
though he would h.avo been more so had he died in America. He
seems by his final words, *' Soyez trauquiiles, messieurs ; c'est mon
sort," not to have regretted being removed from his equivocal
position as a general in arms against his country.
The literature on Moreau is copious, the tiest book being C. Joclmuis, GtruraX
Morcau — Ahriss einer Geschichtf. seines Lebsiis itnd seiner Feldzuge, Berlin, 1814.
A more ordinary work is A. de Eeauchamp, Vie polUiqrte, militaire^ et privi: d»
Giniral Moreau, translated by Pliilippart, London, 1814 ; and there '
tract on his death in Russian, translated into English undi
'.rniiig General Moreait and his Lest Moments, by Paul Sv
title Somt iJ#-
nin, London^
(ILM.&)
MOREL or Moechella. See Mushroom.
MORELIA, formerly Valladolid, a city of Mexico,
capital of the state of Miv'hoacan de Ocampo, is situated
125 miles west by north of Mexico, at a hciL;ln of 6100 feet
above the sea, in 19° 42' N. lat. and 101°" Vv'. long. The
site is a rocky hiE on the Guayangareo valley, and the
western horizon is boimded by the great Quincco mountain
(1 1,000 feet). Since the middle of the century a considerable
extension of the city has taken place, especially towards
the north : its streets, which run for the most part at right
angles to each other, had increased from thirty in 1856 to
ninety-nine in 1873. The principal square is the Plaza
de los Martires (formerly de Armas), where Matamoros
was shot by the Spaniards in 1814 ; its one side is occupied
by the cathedral (1745), a largo building with two towers
about 200 feet high. The churches of the Carmelites (del
Carmen) and San Jose are of some note, and of the nine
convents, now for tho most part in ruins, several were
wealthy and extensive. That of the Capuchins is now
used as a hospital, the old seminary has been turned into
a state-house, and tho tobacco factory, one of the most
ancient buildings in the city, serves as municipal oflices.
An important institution, supported by the state, is the
college of Sau Nicolas de Hidalgo, originally founded by
Juan do San Miguel in the 16th century and rebuilt in
1868. The Ocampo theatre dates from 1869-1870. Water
is brought from a distance of about 3 miles by a fine
aqueduct, constructed in 1788 by D. Antonio de San
Miguel, but tho quality is often deteriorated by tho pre-
sence of vegetable matter. Jlorelia lies tio far from any
great natural route to have much commerce in the present
M O R — M O R
821
Btate'of the couiitiy, aid ite mailufactures are limited to
the production, on a small scale, of cotton, woollen, and silk
goods. A certain delicate sweotjneat called guayabale is
a regular article of commerce to Mexico. In 1750 the city
had about 18,000 inhabitants, in 1873 the municipality
had 36,9-tO and the city proper about 30,000, and in
1880 the number is stated at 20,400.
In 1541 Mendoza chose the Guayangareo valley as the new site
for the city of Michoacan, and in 1545 the place received the name
of ValladoUd. Iturbide and Morelos were both bom within its
precincts ; and in 1823 the Government did this Utter patriot the
honour of renaming the city Morelia. In 1863 it was made the seat
of an archbishop. SeeBol.Soc. degeogr. dela Rep. Jfisr., Mex., 1873.
MORELLET, Andk^ (1727-1819), economist and miscel-
laneous writer, was born at Lyons on the 7th of March 1727.
He was long regarded as almost the last survivor of the
Philosophe school ; and in this character he figures in many
memoirs, — for instance in Madame de Remusat's. He was
educated by the Jesuits in his native town, then at a
seminary in Paris, and finally at the Sorbonne ; and he
took holy orders, but his designation of abbi was the chief
thing clerical about him. He early joined the Philosophe
party, and was a frequenter of most of their salons, being
something of a butt (especially to his fellow-abbi and rival
in political economy, Gfaliani), but having the credit of a
ready and biting pen. Voltaire called him " L'AbbS
Mord-les." His work was chiefly occasional, and the most
notable parts of it were a smart pamphlet in answer to
Palissot's scurrilous play Les Philosophes (which procured
him a short sojourn in the Bastille for an alleged libel on
Palissot's patroness, the princesse de Robeck), and a reply
to Galiani's Commerce dea BUs (1770). Later, he made
himself useful in quasi-diplomatic communications with
English statesmen, and was pensioned, being, moreover,
elected a member of the Academy m 1785. The outbreak
of the Revolution (soon after which he was engaged in a con-
troversy with Chajnfort on the question of the advantages
and deserts of the Academy) did not, as it did with many
of his friends, drive him from the country or put his life
in danger, but it put him in considerable straits of fortune.
He maintained a kind of moderate liberal tone, and the
return of something like order under the Consulate and
the Empire restored him to prosperity and pensions. A
year before his death, at the great age of ninety-two, on the
12th of January 1819 at Paris, he brought out a series of
ifelaTigef, composed chiefly of selections from his former
publications ; and after his death appeared his memoirs,
which are of value for the Philosophe period. Morellet,
though not a man of extraordinary ability or of specially
amiable or estimaUe character, was in both respects a fair
specimen of the man of letters of all work of the time.
He was, in fact, a journalist with a special turn for econo-
mical subjects.
MORERI, Louis. See Encyclop.edia, vol. viii. p. 194.
MORETO, Agustin (1618-1669), Spanish dramatist
and playwright, was born at Madrid in 1618. Of his
personal and even of his literary history little is known.
He studied at Alcala between 1634 and 1639, and after-
wards removed to Toledo, where he entered the household
of the cardinal -archbishop and took holy orders. Ulti-
mately he withdrew altogether from the world, and died a
member of an ascetig religious brotherhood in 1669.
Moreto in his younger years was a prolific writer for the stage,
and almost rivalled Calderon in popularity. Three volumes of his
plays were printed between 1664 and 1681, and many dramas
besides are attributed in whole or in part to him. He employed
all the dramatic forms then in vogue. Of his religious plays, Los
mu Dichoaos ffermanos (The Most Fortunate Brothers), embody-
ing the legend of the seven sleepers, may be mentioned as the least
bombastic and absurd. Others are El Sosario Perseguido, turning
on the persecutions connected with the introduction of the roaary
into Spain, and Maria Egypciaca, a curious representation of the
extraordinary legend of St Mary of Egypt His heroic drama, Et
ValicnU Justiciero (The Brave Justiciary), a story of the times of
Pedro the Cruel, is one of (rcnsiderable power. His *' comedias
de figuron," or "character comedies," as they are called (compare
vol. viL p. 422), include El Lindo Don Diego (The Handsome
Don Diego) and El Desden eon tl Dcsden (Disdain met ^ith
Disdain), the latter partly borrowed from Lope de Vega's Milagros
del Desprecio, and m turn imitated by Moli^re (in his Prinasse
d'^lide), by Carlo Gozzi {PTincipcssa Filoso/a), and by Schreyvogol
{Donna Diana). The Comedias Escogidas de Don Agustin Moreto
y Cabaila form the 39th volume of the BiblioUca de Autores Espa-
Holes (Madrid, 1856).
MORETTO, II (" The Blackamoor," a term which has
not been particularly accounted for), is the name currently
bestowed upon AlessandkoBonvicino(1498-c. 1560), acelo-
brated painter of Brescia, Venetian schooL He was bom
at Rovato in the Bresciau territory in 1498, and studied
first under Fioravante Ferramola of Brescia, afterwards,
still youthful, with Titian in Venice. His own earlier
method, specially distingmshed by excellent portrait-paint-
ing, was naturally modelled on that of Titian. Afterwards
he conceived a great enthusiasm for Raphael (though he
does not appear to have ever gone to Rome), and his style
became partially Raphaelesque. It was, however, novel in
its combina'tion of diverse elements, and highly attractive, —
with fine pencilling, a rich yet not lavish use of perspective
and decorative effects, and an elegant opposition of light
and shade. The human figure is somewhat slender in
Bonvicino's paintings, the expression earnestly religious,
the flesh-tints varied, more so than was common in the
Venetian school. The backgrounds are generally luminous,
and the draperies well modified in red and yellow tints
with little intermixture of blue. The depth of Bonvicino's
talent, however, was hardly in proportion to its vigour
and vivacity ; and he excelled more in sedate altar-pieces
than in subjects of action, and more in oil-painting than
in fresco, although some fine series of his frescos remain,
especially that in the villa Martinengo at Novarino, near
Brescia. Among his celebrated works in the city are — in
the chiu'ch of S. Clemente, the Five Virgin Martyrs, ind
the Assumption of the Madorma (this latter may count as
his masterpiece) ; in S. Nazaro e Celso, the Coronation of
the Madonna ; in S. Maria delle Grazie, St Joseph ; in S.
Maria de' MiracoU, St Nicholas of BarL In the Vienna
Gallery is a St Justina (once ascribed to Pordenone) ; in
the Stadel Institute, Frankfort, the Madonna enthroned
between Sts Anthony and Sebastian ; in the Berlin Museum,
a colossal Adoration of the Shepherds, and a large votive
picture (one of the master's best) of the Madonna and
Child, with infant angels and other figures above the
clouds, and below, amid a rich landscape, two priests ; in
the London National Gtallery, St Bernardin and other
saints, and two impressive portraits. H Moretto is stated
to have been a man of childlike personal piety, preparing
himself by prayer and fasting for any great act of sacred
art, such as the painting of the Virgin-mother. His dated
works extend from 1524 to 1554, and he was the master of
the pre-eminent portrait-painter Moroni. His death took
place towards 1560.
MORGAGNI, GiovAJon Battista (1682-1771), the
founder of pathological anatomy, was born 25th February
1682 at Forli, an ancient and important toivn on the
.iEmiUan road southwards from Bologna. ^ His parents
were in comfortable circumstances, but not of the nobility;
it appears from his letters to Lancisi that Morgagni was
ambitious of gaining admission into that rank, and it may
be inferred that he succeeded from the fact that he is
described on a memorial tablet at Padua as "nobilis
Forolensis." At school he was conspicuous for his talentSj
and he was especially noted for his readiness in classical
epigram. At the age of sixteen he went to Bologna to
• A statue of the illustrious citiwn was erected at Forll in 1875, and
the town library preserves fourteen MS. volumes of his writings.
822
M 0 R G A G N I
studj' philosophy and medicine, and he graduated with
much 6clat as doctor in both faculties three years later
(1701). He acted as prosector to Valsalva (one of the
distinguished pupils of Malpighi), who held the office of
" demonstrator anatomicus " in the Bologna school. He
assisted Valsalva more particularly in preparing his cele-
brated work on the Anatomy and Diseases of the Ear, which
came out in 1704. Many years after (1740), Morgagni
edited a collected edition of Valsalva's writings, with im-
portant additions to the treatise on the ear, and with a
memoir of the author. When Valsalva was transferred
to Parma Morgagni succeeded to his anatomical demon-
stratorship. At this period he enjoyed a high repute
in Bologna ; he was made president of the Academia
Inquietorum when in his twenty- fourth year, and he
is said to have signalized his tenure of the presiden-
tial chair by discouraging abstract speculations, and by
Betting the fashion towards exact anatotriical observa-
tion and reasoning. He published the substance of his
communications to the Academy in 1706 under the title
of Adversaria Anaiomira, the first of a series by which
ho became favourably known throughout Europe as an
accurate anatomist ; the book included " Observations
on the Larynx, the Lachrymal Apparatus, and the Palvic
Organs in the Female." After a time he gave up his
post at Bologna, and occupied himself for the next two
or three years at Padua and Venice with anatomical
studies (of fishes at the latter city), as well as with
chemistry and pharmacy, and vnth reading in the libraries.
He then settled in practice in his native town, and soon
attracted a large amount of business ; there was hardly a
case of much difSculty about which he was not consulted
even by the older physicians, " adeo erat in observando
attentus, in prsedicendo cautua, in curando felix." Such
at least is the contemporary eulogy. After less than three
years of this career, which he found fatiguing, he sought
an opportunity of returning to more academical work.
At Padua he had a friend in the elder Guglielmini, pro-
fessor of medicine, but better known as a writer on physics
and mathematics, whose works he afterwards edited (1719)
with a biography. Guglielmini desired to see him settled
as a teacher at Padua, and the unexpected death of
Guglielmini himself made the project feasible, VaUisnieri
being transferred to the vacant chair and Morgagni suc-
ceeding to the chair of theoretical medicine. He came to
Padua in the spring of 1712, being then in his thirty-first
year, and he taught medicine there ^vith the most brilliant
success until his death sixty years later (6th December
1771). When he had been three years in Padua an oppor-
tunity occurred for his promotion (by the Venetian senate)
to the chair of anatomy, in which he became the successor
of an illustrious line of scholars, including Vesalius,
Fallopius, Fabricius, Gasserias, and Spigelius, and in which
he enjoyed a stipend that was increased from time to time
by vote of the senate until it reached twelve hundred gold
ducats. Shortly after coming to Padua he married a lady
of Forli, of noble parentage, who bore him three sons and
twelve daughters ; of the daughters, four died in infancy,
and the other eight took the veil as they grew up ; of the
sons, one died in boyhood, one entered the Jesuit order,
and the eldest settled at Forli, where he married and lived
to the age of fifty-two, predeceasing his father by five years
and leaving a family to his care. Morgagni enjoyed an
unequalled popularity among all cla.s.ses. He was of tall
and dignified figure, with blonde hair and blue eyes, and
with a frank and hajjpy expression ; his manners were
polished, and he was noted for thi elegance of his Latin
style. Ho lived in harmony with his colleap^ics, who are
said not even to have envied him 'ais unprcccdentedly large
stipend ; his house and lecture theatre were frequented
." tanquam officina s.ipientiaj " by students of all agea
attracted from all parts of Europe ; he enjoyed the friend-
ship and favour of distinguished Venetian senators and of
cardinals ; successive popes conferred honours upon hini ;
and on two occasions when a hostile army occupied the
jEmil'a his house was ordered to be treated with the same
marked distinction that the great Emathian conqueror
showed to the house of Pindar. Before he had been long
in Padua the students of the German nation, of all the
faculties there, elected him their patron, and he advised
and assisted them in the purchase of a house to be a
German library and club for all time. No person of any
learning came to Padua without seeing and conversing
with Morgagni, and no one ever left him without admiring
equally his character and his teaching. One of his bio-
graphers and editors, the celebrated Tissot of Lausanne,
observes that he had met with several Englishmen re-
turning from Italy who told with pleasure and gratitude
"quam hnmaniter Ulos exceperat, et quantum ex illius
coUoquiis, doctis, variis, jucundis profecerant." He was
elected into the Imperial Caesareo-Leopoldina Academy in
1708 (originally located at Schweinfurth), and to a higher
grade in 1732, into the Eoyal Society in 1724, into the
Paris Academy of Sciences in 1731, the St Petersburg
Academy in 1735, and the Berlin Academy in 1754.
Among his more celebrated pupils were Scarpa (who died
in 1832, connecting the school of Morgagni with the
modern era), Cotunnius (Cotugno), and Caldani, the author
of the magnificent atlas of anatomical plates published in
4 vols, at Venice in 1801-1814.
Meanwliile he published on a variety of subjectd. In bis earlier
years at Padua be brought out (1717-1719) five more series of tbe
Adversaria Anaioviica oy wbicb bis reputation was first made ;
but for more tban twenty years after tbe last of tbese his strictly
medical publications were few and casual (on gall-stoues, varices of
the vena cava, cases of stone, and several memoranda on medico-legal
points drawn up at the request of the cui-ia). Classical scholarsliip
in those years occupied bis pen more tban anatomical observations ;
and the reason of this appears to have been that he spent the
summer months in the country for the sake of his health, and occupied
his leisure with literary studies. His writings in this class include
letters to Ijancisi on the m.onner of Cleopatra s death, commentaries
on Celsus and Sammonicus, notes on Pi'osper Alplnus, Varro,
Vegetius, Columella, and Yitruvius, and antiquarian researches
into tbe topography of the country round Ravenna and bis own
birthplace (Forum Livii). His edition of tbe worts of Valsalva,
published in 1740 (in 2 vols. 4to) with plates, occupied much of
nis time, being enriched with a life and a commcntai-y, and with
many additional observations of bis own. It was not until 1761,
when ho was in bis eightieth year, that be brought cut tbe great
work which, once for all, made pathological anatomy a science,
and diverted tbe course of medicine into new channels of exactness
or precision — the Dc Scdibus ci Causis Morhorvm per Anatomem
indagalis. He died on 6tb December 1771. During the preceding
ten years tbe Ds Scdilnts, notwithstanding its bidk, was reprinted
several times (thrice in four years) in its original Latin, and was
translated into French (1765), English (1769, 3 vols. 4to), and
German (1771). Some account of this remarkable work remains
now to be given.
The only special treatise on pathological anatomy previous to that
of Morgagni was the work of Th^opbile Bonet of Ncucbatcl, Scjatl-
ckrctitvi : sire Anatomia practiea ex endavcrillis iiiorho dcnafis, lil-st
published (Geneva, 2 vols, folio) in 1679, three yeara before Morg:;gni
was boi-n ; it was republished at Geneva (3 vols, folio) in 1700, and
again at Leyden in 1709. Although the normal anatomy of the
body bud been comprcbensivoly, and in some parts exhaustively
Vrittcn by Vesalius and Fallopius, it bad not occurred to any one
to examine and describe systematically the anatomy of dise^iscd
origans and parts. Harvey, a century after Vesalius, n.iivcly re-
marks that tliero is more to bo learned from the dissection of one
person who bad died of consumption or -other clironic malady tban
from the bodies of ten persons who had been hanged. Glisson
indeed (1597-1677) shows, in a pass.ago quoted by Bonet in the
preface to tbe Sepulehrctum, that bo was familiar vrith the idea,
at least, of systematically comparing tbe state of the organs in a
series of cadavera, and of noting those conditions which invariably
accompanied a given set of symptoine. Tbe work of Bonet was,
however, tho first attempt at a system of morbid anatomy, ard,
although it dwelt mostly upon curiosities and monstrositios, it
M O R— TVI 0 R
823
oyoyed much repnte in its day ; Haller speaks of it as " an im-
mortal work, which may in itself servo for a pathological library. "
'Morgagni, in the preface to his own work, discusses the defects and
merits of the SepulchrUum ; it was largely a compilation of other
men's cases, well and ill authenticated; it was prolii, often inaccurate
.and misleading from ignorance of the normal anatomy, and it was
wanting in What womd now be called objective impartiality, — a
quality which was introduced as decisively into morbid anatomy
by Morgagni as it had been introduced two centuries earlier into
normal liuman anatomy by Vesalius. Morgagni has narrated .the
circumstances under which the De Scdibus took origin. Having
finished Ma edition of Valsalva in 1740, he was taking a holiday in
the country, spending much of his time in the company of a young
friend who was curious in many branches 'of knowledge. The
conversation turned upon the Sepulchretum of Bonet, and it was
suggested to Morgagni by his dilettante friend that he should put
on record his omti oBservations. It was agreed that letters on the
anatomy of diseased organs and parts should bo written for the
perusal cf this favoured youth (whose name does" not transpire) ;
and they were continued from time to time unti^ they numbered
seventy. Those seventy letters constitute the De SedilM el Causia
Morbonim^ which was given to the world as a systematic treatise
in 2 vols, folio, Venice, 1761, twenty years after the task of epis-
tolary instruction was begun. The letters are arranged in five
books, treating of the raorWd conditions of the body a capiU ad
calcem. The five books are dedicated respectively to Trew, Brom-
field, Senac, Schreiber, and Meckel, as representing the several
learned societies of which Morgagni was a foreign member. The
five books together contain, according to an enumeration by the
present writer, the records of some 640 dissections. Some of these
».-e given at great length, and \vith a precision of statement and ex-
haustiveness of detail hardly surpassed in the so-called "protocols "
of the German pathological institutes of the present time ; others,
again, are fragments brought in to elucidate some question that had
arisen. The symptoms during the course of the malady and other
antecedent circumstances ace always prefixed with more or less ful-
ness, and discussed from the point of view of the conditions found
after death. Subjects in all ranks of life, including several cardinals,
figure in this remarkable gallery of the dead. Many of the cases
are taken from Morgagni's early experiences at Bologna, and from
the records of his teachers Valsalva and Albertini not elsewhere
published. Those six hundred or more cases are selected and
arranged with method and purpose, and they are often (and some-
what casually) made the occasion of a long excursus on general
pathology and therapeutics. Tbe range of Morgagni's scholarship,
as evidenced by his references to early and contemporary literature,
strikes one \vith astonishment. It has been contended that he was
himself not free from prolixity, the besetting sin of the learned ; and
artaiuly the form and aiVangement of his treatise are such as to
make it difficult to use in the present day, notwithstanding that it
is well indexed in the original edition, in that of Tissot (3 vols.
4to, Yverdun, 1779), and in more recent editions. It differs from
modern treatises in so far as thQ symptoms determine the order and
manner of presenting the anatomical facts. Although Morgagni was
the first to understand and to demonstrate the absolute necessity of
basing dia^osis, prognosis* and treatment on an exact and com-
prehensive Knowledge of anatomical conditions, he made no attempt
(like that of the Vienna school sixty years later) to exalt pathological
anatomy into a science disconnected from clinical medicine and
remote from practical needs. His orderliness of anatomical method
(irapl}'ing his skill with the scalpel), his precision, his exhaustive-
ness, and his freedom from bias are his essentially modern or
scientific qualities ; his scholarship and high consideration for
classical and foreign work, his sense of practical ends (or his common
sense), and the breadth of his intellectual horizon prove him to
have lived before medical science had become largely technical or
mechanical. It is clear that Morgagni's immense personal influence
during his lifetime did not alone make his book famous ; at a
distance of two hundred years from his birth, and more than one
hundrcil from his death, the opinion is unanimous that his treatise
was the commencement of the era of steady or cumulative progress
in pathology and in practical medicine. SjTnptoms from that time
ceased to be made up iuto more or less conventional groups, each
of wliich was a disease ; on the other hand, they began to be viewed
as *' the cry of the suffering organs," and it now became possible to
develop Sydenham's gi-and conception of a natural history of disease
in a catholic or scientific spirit. Laennec'sapplication of the stetho-
scope to detect the sounds given out in diseased states of the heart
and lungs, and Bright's application of the test-tube and re-agents
to reach the structural and functional conditions of tbe kidney
through the state of the urine, were the direct results of ilorgagni's
endeavour to lay bare the seats and causes of disease by anatomy ;
and those two" means of diagnosis are the daUy and hourly resource
of every modem practitioner. In more general terms, Morgagni's
work substituted localization for generalization and precision for
vagueness.
. A biography of Morgagni by Mosca was published at Kaplrs is 176S. Els
MORGAN, Sydney Owenson, Lady (1777^-1859),
novelist and miscellaneous describer and critic, was one of
the most vivid and hotly-discussed literary personages of
her generation. She was the daughter of an Irish actor,
but it was one of her whims to keep the year of her birth
a secret ; " once upon a time " on Christmas day was her
answer to inquiries. She began her literary career with a
precocious volume of poems. Her second venture, St Clair
(1804), a novel of ill-judged marriage, ifl^tarred love, and
impassioned nature-worship, in which the influence of
Goethe and Eousseau was apparent, at once attracted
attention. Another novel, The Soviet of St Dominick
(1806), was also praised for its qualities of copious imagina-
tion and description, though the critics were inclined to
nibble at the writer's grammar. But the book which
made her reputation and brought her name into warm con-
troversy was The Wild Irish Girl, also published in 1806.
In this she-ap'peared as the ardent champion of her native
country, a politician rather than a novelist, extolling the
beauty of Irish scenery, the richness of the natural wealth
of Ireland, the noble traditions of its early history, and
sketching types of the various classes with direct refer-
ence to the misgovemment to which she traced their evil
features. She followed this up with Patriotic Sketches and
Metrical Fragments in 1807, fitting some Irish melodies with
words ("Kate Kearney" among the number) in the same
year in which Moore began a similar task. Miss Owen-
son's politics and the favour shown her by the Whig
aristocracy probably prompted the savage attack made
upon her next novel, Ida, a Woman of Athene, in the first
number of the Quarterly {\9Q'Si). From first to last her
style was open to the reproach of being made up too much
of quotations, and her grammar was not always correct ;
but exuberant humour, keen wit, and fertility in the inven-
tion of striking and romantic incidents carry any unbiassed
reader easily over all minor faults of composition. Her
great ambition was to draw vivid pictures of the mingled
" mirth and misery, ferocity and fun," of the Irish under
English rule, and she succeeded. Her novels sufi'er as
stories from this political purpose ; she drags in too many
character-sketches, and, though they ere al^-ays drawn
with vivacity and sharp penetration, they are drawn with
too much bias of romantic enthusiasm on the one side
and satirical spite on the other. In. 1812 she was married
to Sir T. C. Morgan, but books still continued to flow
from her facile pen. In 1814 she produced her best
novel, O'DonneL, a decided advance on previous work.'
She published an elaborate study of France under the
Bourbon restoration in 1817. This was' attacked with
outrageous fury in the Quarterly, the authoress being
accused of Jacobinism, falsehood, licentiousness, and im-
piety. She took her revenge indirectly in the novel of
Florence Macarthy (1818), in which a Quarterly reviewer,
Con Crawley, is insulted with supreme feminine ingenuity.
Italy, a companion work to her France, was published in
1821 ; Lord Byron bears testimony to the justness of its
pictures of life. The results of Italian historical studies
were given in her Life and Times of Salvator Rosa (1824).
Then she turned again to Irish manners and politics with
a matter-of-fact book on Absenteeism (182.5), and a highly
stirring and romantic novel. The O'Briens and the O'Fla-
hertys (1827). The Book of the Boudoir (1829) consisted
of miscellaneous reflexions and reminiscences. Under the
ministry of Lord Grey Lady Morgan obtained a pension of
£300. During the last thirty years of her long life she
broke no new ground, but to the last she was an entertain-
ing writer, and sent some sprightly verses to the Atlienesitm
824
M O R — M O R
in January 1859, a few weeks before her deatli, protesting
against being called old. Tlie titled of lier books in this
period are : — France in 1829-30, Dramatic Scenes from Real
Life (1833), Tlie Princess (1835), JVoman and her Master
(1840), The Book ivilhoui a Name (1811), Passages from
my Autobiography (1859). More of her autobiography
and many interesting letters were edited ■iWth a memoir by
Hepworth Dixon in 18G2. He respected her prejudice
against disclosing her exact age.
MORGANATIC MAERIAGE. Sea Maeeiage.
MORGHEN, Raffaello Sanzio (175S-1833), a distin-
guished engraver, was born at Naples on 19th June 1758.
He received his earliest instructions from his father, him-
self an engraver ; but, in order to be initiated more fully
in "the art, he was afterwards placed as a pupil under the
celebrated Volpato. He assisted this master in engraving
the famous pictures of Raphael in the Vatican, and the
print which represents the miracle of Bolsena is inscribed
xvith his name. He married Volpato's daughter, and, being
invited to Florence to engrave the masterpieces of the
Florentine gallery, he removed thither with his wife in
1782. His reputation now became so great as to induce
the artists of Florence to recommend him to the grand-duke
as a fit person to engrave the Last Supper of Leonardo
da Vinci ; apart, however, from the dilapidated state of
the picture itself, the drawing made for Morghen was
unworthy of the original, and the print, in consequence,
although an admirable production, fails to convey a correct
idea of the style and merit of Leonardo. Morghen's fame,
however, soon extended over Europe ; and the Institute of
France, as a mark of their admiration of his talents, elected
him an associate in 1803. In 1812 Napoleon invited
him to Paris and paid him the most flattering attentions.
He died at Florence on 8th April 1833.
A list of the artist's woiks, published at Florence in 1810, com-
piised 200 compositions ; the number was afterwards considerably
increased. Amongst the most remarkable, besides those already
mentioned, may be noticed the Transfiguration from Raphael, a
Magdalen from jMurillo, a Head of the Saviour from Da Vinci, the
Car of Aurora fi-om Guide, the Hours and the Repose in Egypt
from Poussin, the Pri^e of Diana from Domenichino, the Monument
of Clement XIII. from Canova, Theseus vanquishing the Minotaur,
Francesco Moncado after Vandyke, portraits of Dante, Petrarch,
Ariosto, Tasso, and a number of other eminent men. His prints
have hardly maintained the reputation which they enjoyed during
the artist's lifetime. Though carefully and delicately executed, they
are somewhat mechanical and wanting in force and spirit.
MORHOF, Daniel Geoeo (1639-1691), the learned
author of a survey of universal literature entitled Polyhislor
sive de anctorum notitia et rerum commenlarii, was born at
Wismar in 1639, studied law at Rostock, and was appointed
professor of poetry there in 1660. In 1665 he went to
the new university of Kiel as professor of eloquence and
poetry ; this chair he exchanged for that of history in 1673.
He died at Liibeck in 1691. Of his numerous writings
only the Polyhistor continues to be of value to the literary
historian as a bibliographical work displaying judgment
as well as knowledge. The first seven books (Polyhistor
Literarius) appeared in 1688-1698 ; the publication of the
two remaining parts (P. Philosophicus and P. Practicus)
was completed by MoUer in 1707. The best edition is
that of A. Fabricius (2 vols. 4to, Leipsic, 1747).
MORIAH. In 2 Chron. iii. 1 wo read that Solomon
built the Temple at Jerusalem on Mount Moriah (in
nj'litsri). Xhis name for the Temple hill, the ancient Zion,
is not found elsewhere in the Old Testament, and can
hardly have been a current one. But a mountain in the
" land of Moriah " was the place where Abraham was com-
manded to sacrifice Isaac ; Josephus (Ant., i. 13, 2) assumes
that this Mtipiov opoi was the Temple hill, and the same
view is expressed in the Targums, where it is exegetically
baKd on the obscure verse, Gen. uaL 14 (comp. Jerome,
Qusest. ffeb. in Gen. xxii. 2). Probably this traditiotf
already existed in the time of the Chronicler, who appears
to connect the name etymologically vrilh Jehovah's mani-
festation of himself, as is done in Gen. xxii. 14.1
Jerome repeatedly calls the Temple hiU Mount Moriah, but the
cunency which the name has with modem writers is mainly due
to the erroneous identification of Zion with the western hill beyond
the TyropcEon. In Christian tradition the place of Isaac's sacrifice
was identified with Calvary {see Theodosius, Dc Situ Terra: Sands),
and it is now shown in a chapel adjoining the church of the Holy
Sepulchre.
MORIER, James (1780-1 849), traveUer and author, was
born in 1780. Through the influence of his uncle Admiral
William Waldegrave, Baron RaJstock, he at an early period
entered the diplomatic service, and as secretary to Lord
Elgin followed the grand' vizier in the Egyptian cam-
paign. An account of his Eastern experiences was pub-
lished in 1812, under the title A Journey through Persia,\
Armenia, and Asia Minor to Constantinople in 1 808-9. From
1810 to 1816 he was the English representative at the
court of Persia, and after his return he published A Second
Journey through Persia to Constantinople between the years
1810 and 1816. His knowledge of Eastern life and man-
ners he also turned to account in the composition of several
entertaining romances, displaying some skill in the deline-
ation of Oriental scenery and character, and considerable
powers of wit and humour. The most popular of these
were: — The Adventures of Hajji Baba of Ispahan, 1824;
The Adventures of Hajji Baba of Ispahan in England,
1828 ; Zohrab the Hostage, 1832 ; and Ayesha the Maid of
Ears, 1834. Morier died at Brighton, 23d March 1849.
MORILLON, a name commonly given by fowlers to
the female or immature male of the Goldex-Eye (vol. x.i
p. 757), the Clangula glaucion of modern ornithology,'
under the belief which still very generally obtains among-
them, as it once did among naturalists, that they formed a
distinct species of Duck. The mistake no doubt originated
in, and is partly excused by, the facts that the birds called
Morlllons were often of opposite sexes, and differed greatly
from the adult male Golden- Eye, whosefull and beautiful plu-
mage is not assumed until the second year. The word is used
in French in precisely the same form, but is m that language
applied to the Tufted Duck, Fuligula cristata, and is derived,
according to Littr^, from more, signifying black, (a. n.)
MORIN, Jean, or, in Latin, Joannes Moeinus (1591-
1659), the most learned Catholic theologian of his time and
one of the founders of Biblical criticism, was born in 1591
at Blois of Protestant parents, acquired Latin and Greek at
Rochelle, and continued his studies at Leyden. Immersed
in Biblical and patristic lore, he began to waver in his
Protestantism, and moved to Paris, where he made many
friends in literary circles, particularly Cardinal Du Perron,
to whom his conversion to Catholicism is ascribed. In
1618 he joined the recently formed Parisian Oratory,
where he could give himself to quiet study, and in due
course took priest's orders. In 1625 he visited England
in the train of Henrietta Maria, and in 1640 he was at
Rome, on the invitation of Cardinal Barberini, and -was
received with special favour by Pope Urban \r[II., who
employed him on the commission for forwarding his pro-
ject of union with the Eastern Chiu-ch. He was, however,
soon recalled to Paris by Richelieu, and the rest of his life
was spent among books in incessant literary labour, his
health, memory, and intellectual vigour remaining unim-
paired even in old age. His pen sometimes brought him
into trouble. The Histoire de la dclivrance de l'£glite
Chretienne par I'emp. Constantin. et de la grandeur et
souveraineie temporelle donJiee a VEglijiC Eomaine par Ics
rois de France (1630) gave great offence at Rome, and a
' The word Moriah, however, can hanlly eome from nsi, " see ; " it
ia perhaps akin to Moreb, "revealer," "Icfchcr.*^
M O R— M O R
825
Declaration (1654), directed against faults in the adminis-
tration of the Oratory and reflecting on the general (Father
Bourgoing), was strictly suppressed. So, too, his great work
on penance gave equal offence to the Jesuits and to Port^
Koyal, and even after his death (1659) the polemical
vehemence of his Exercitationes Biblicse, and the exaggera-
tion of his assertion "apud neotericos Haereticos verba
Scripturarum non esse Integra, non superficiem, non folia,
nedum sensum, medullam et radicem rationis" long led
Protestants to treat his valuable contributions to the history
of the Hebrew text as a mere utterance of Popish prejudice.
Moiinus was a voluminous and prolix writer on ecclesiastical
antiquities. His principal works in this field are Comtnentarius
tiL'toricus de disciplina in adininistraiione sacramenti paenitcntim
XIII primia scculis in Eccl. Occid. et kucusque in Orient, ohservata
(1651), and C<nmn. de sacris Ecdcsim ordinationibus seatndum
tintigucs et rccentiores Latinos, Grmcos, Syros et Bahylonios (1655).
TLo second of these works expresses those irenical views on the
«ul>jcct of ordination which recommended Morinus to Urban VIII.
The liteiarj correspondence of Moiinus appeared in 1682 under
the titlt of Andquitalcs Ecclesia Orientalia (edited by R, Simon).
The chief fame of llorinus, however, now rests on his Biblical
and critical labours. By his cdiiio princcps of the Samaritan Penta-
teuch and Targum, in the Palis Polyglott, he gave the first impulse
in Em ope to the study of this dialect, which he acquired without
a teacher (framing a grammar for himself) by the study of ilSS.
then newly brought to Europe. Not unnaturally he formed a very
exaggerated view of the value of the Samaritan tradition of the text,
exalting it above the tradition of the Jews {Exercilationes in utruTn-
que Samarilanorum fentatcuclutm, 1631). A similar tone of ex-
aggerated depreciation of the Hebrew text, coloured, as has been
remarked above, by polemical bias against Protestantism, mars his
greatest work, the posthumous Excvcitationes hiblicss de Hcbraici
Orseciqne texiiia sinceritate (1660), in which, following in the foot-
steps of Cappellus, but with incomparably greater learning, he brings
irrefragable arguments against the then current theory of the
absolute integrity of the Hebrew text of the Old Testament, and
the antiquity of the vowel points. The second part of this work
is still valued as a copious storehouse of materials for the hiatory
of the Hebrew text collected by the most self-denying labour —
t)iei3 ingraiiis, as he said himself.
MORLAIX, the chief town of an arrondissement in the
department of Finistfere, France, lies 350 miles west of
Paris on the railway from Paris to Brest, and at the con-
fluence of two small streams, 7 miles distant from the sea.
Its port has 13 feet of water at ordinary and 23 feet at
spring tides. The entrance of the roadstead is defended
by the Chateau du Taureau, which stands on a rock in the
sea, and was built in 1512 to protect the town from the
English. Morlaix still contains a considerable number of
curious wooden houses of the 15th, 16th, and 17th centuries;
tut the most striking piece of architecture in the town is
"the gigantic two-storied viaduct of the railway from Paris
to Brest, 931 feet long and 207 feet above the quays.
The old church of the Dominicans is now occupied by the
town library. The hospital has beds for 500 patients,
and can accommodate 300 female lunatics besides. A
tobacco-factory, employing 400 men and 700 women, is
the principal industrial establishment ; and there are also
€xtensive paper-mills, a considerable flax-mill, canvas-fac-
tories, foundries, and saw-mills. A considerable trade is
carried on in grain, yarn, canvas, leather, tallow, wax, and
horses; and a large quantity of butter, cattle, and vegetables
is exported from Roscoff, a village in the neighbourhood,
which is also known for its sea-bathing and its zoological
station. The population of Morlaix was 15,183 in 1876.
Judging by the numerous coins found on the spot, the site of
ilorlaix was probably occupied in the time of the Romans. The
founts of Leon held the lordship in the 12th century, but the
dukes of Brittany disputed pos.sessiou with them, and in 1187 Henry
II. of England, guardian .of Arthur of Brittany, made himself master
of the town after a siege of several weeks. During the War of the
Hundred Years Morlaix was again captured and recaptured by the
French and the English, and pillaged by the latter in 1522. Queen
Jlary of Scotland, on her way to be married to the Dauphin, made
Bolcnin entry into Jlorlaix in 1548. And finally, the town having
joined the League, the castle was taken by storm in tho name of
Henry IV. in 1594.
MORLAND. Geoege (1763-1804), animal and subject
painter, was bom in London on the 26th of June 1763. He
came of a race of artists. His father, a painter, mezzotint-
engraver, and picture-dealer, gave him a caTefuI art-training,
and at sin exceptionally early age he produced works of
wonderful promise. At sixteen he exhibited sketches at
the Tloyal Academy, and even before this his productions
found ready purchasers, and some of them had been
engraved. But already the taste for dissipation, which
was stronger in Morland than even his love for art, had
begun to manifest itself, and at seventeen he escaped from
the over-strict discipline of his father's house, and began
a career of reckless prodigality which has hardly a parallel
in art-biography, gathering round him an entourage of the
most abandoned associates, and supporting himself by tho
sale of the pictures^rustic subjects and scenes from low
life — which he threw off with unexampled rapidity. About
1786 there appeared to be some prospect of amendment.
He went to reside at Kensal Green, came under the influ-
ence of better companions, and married a beautiful and
virtuous girl, a sister of James Ward the animal-painter
and William Ward the engraver. The subjects which
Morland painted during this period reflect the change in
his way of life. The Idle and Industrious Mechanic,
and Letitia or Seduction, moralities in the style of
Hogarth, were engraved and became exceedingly popular.
But soon the force of old habit asserted itself, the desire
for freedom and lawlessness returned to the artist with
redoubled violence, and he again drifted into a career of
riot and intemperance. The means of dissipation were
not wanting ; the dealers were eager for his productions ;
indeed, so greatly were they esteemed that skilled copyists
were employed to make many transcripts fr(Jm the pictures
on which he was at work, which were sold as originals to
an vmsuspecting public. The finest of Morland's subjects
date from 1790 to 1792. In 1791 was painted the Inside
of a Stable, now in the National Gallery, probably the
artist's masterpiece. In spite of his popularity and his
industry his affairs became inextricably embarrassed. For
a trme he eluded the bailiffs with singular dexterity, but
in TTovember 1799 he was arrested. Obtaining the Rules
of the Bench, he took a house ivithin bounds, and con-
tinued to practise both his art and his debauchery. He
was released under the Insolvent Act of 1802, but hia
health was ruined and he was speedily stricken with palsy.
Partially recovering, he continued to paint, but before long
he was again arrested for debt, and died in a sponging-
house in Eyre Street, Coldbath Fields, on the 29th of
October 1804. His wife survived him only some three
days, and they were buried in one grave.
The most characteristic works of Morland are those which deal
with rustic and homely life. They show much direct and instinct-
ive feeling for nature, and admirable executive skill, but they have
no elevation of subject, no gi-eat beauty of colour or truth of atmo-
sphere. They sufler from the haste in which the artist habitually
worked. Many of them have been admirably mezzotinted by J.
R. Smith and his pupils, William Ward and John Young, Par-
ticulare of Morland's life will be found in the biogl-aphies by J.
Hasscll (1804), G. Dawe (1807), and Blagton (1806), and in Memoirs
of a Picture, by W. Collins, 1805.
MORMONS, or The Church of Jesus Christ of Latter-
Day Saints, are a religious sect founded by Joseph Smith
at ilanchester. New York, in 1 830, and for the last thirty-
six years settled in Salt Lake City, Territory of Utah,
United States. Smith was born 23d December 1805 at
Sharon, Windsor county, Vermont, fron, which place ten
years later his parents, a poor, ignorani, thriftless, and
not too honest couple, removed to New li' ork, where they
settled on a small farm near Palmyra, Wayne county
(then Ontario). Four years later, in 180)9, they removed
to Manchester, sotofe 6 miles off; and it ^^ai at the latter
place when fifteen years old that Joseph 6t,san to have]
XVL -r.i04
826
MORMONS
his alleged visions, in one of which on the night of 2l8t
Beptember 1823 the angel Moroni appeared to him three
times, and told him that the Bible of the Western Continent,
the supplement to the Now Testament, waa buried in a
certain spot near Manchester. Thither, four years later
and after due disciplinary probation. Smith went, and had
delivered into his charge by an angel of the Lord a stone
hox, in which was a volume, 6 inches thick, made of thin gold
plates 8 inches by 7, and fastened together by three gold
rings. The plates were covered with small writing in the
" reformed Egyptian " tongue, and were accompanied by a
pair of supernatural spectacles, consisting of two crystals
Bet in a silver bow, and called " Urira and Thummim ; "
by aid of these the mystic characters could be read.
Being himself unable to read or write fluently. Smith
employed as amanuensis one Oliver Cowdery, to whom,
from behind a curtain, he dictated a translation, which,
"with the aid of a farmer, Martin Harris, who had more
money than Avit, was printed and published in 1830 under
the title of Th'e Book of Mormon^ and accompanied by the
Bwom statement of Oliver Cowdery, David Whitmer, and
Martin Harris that an angel of God had shown them the
plates of which the book was a translation. This testi-
mony all three, on renouncing Mormonism some years
later, denounced as false ; but meanwhile it helped Smith
to impose on the credulous, particularly in the absence of
the gold plates themselves, which suddenly and mysteri-
ously disappeared. The Booh of Mormon, in which Joseph
Smith was declared to be Grod's " prophet," with all power
and entitled to all obedience, professes to give the history
of America from its first settlement by a colony of refugees
from among the crowd dispersed by the confusion of tongues
at the Tower of Babel down to the year 5 a.d. These settlers
having in course of time destroyed one another, nothing
of importance occurred until 600 B.C., when Lehi, his ivife,
and four sons, with ten friends, all from Jerusalem, landed
on the coast of Chili. All went well until the death of
Lehi, when the divine appointment to the leadership of
Nephi, the youngest son, roused the resentment of his
elder brothers, who were in consequence condemned to
have dark skins and to be an idle mischievous race, — hence
the North-American Indians. Between the Nephites and
the bad Hebrews a fierce war was maintained for centuries,
until finally, in spite of divine intervention in the person
of the crucified Christ, the Nephites fell away from the
true faith, and in 384 a.d. were nearly annihilated by
their dark-skinned foes in a battle at the hill of Cumorah,
in Ontario county. New York. Among the handful that
escaped were Mormon and his son Moroni, the former of
whom collected the sLxteen books of records, kept by suc-
cessive kings and priests, into one volume, which on his
death was supplemented by his son ■(vith some personal
reminiscences and by him buried in the hill of Cumorah, —
he being divinely assured that the book would one day be
discovered by God's chosen prophet. This is Smith's
account of the book ; but in reality it was written in 1812
as an historical romance by one Solomon Spalding, a crack-
brained preacher ; and the MS. falling into the hands of an
unscrupulous compositor, Sidney Rigdon, was copied by him,
and subsequently given to Joseph Smith. Armed with
this book and witl> self-assumed divine authority, the latter
Foon began to attract followers. On 0th April 1830 the
fir:-t coftference of the new sect, called by their neighbours
Mormons, but by themselves subsequently Latter-Day
Saints of Jesus Christ, was held at Fayette, Seneca county.
New York, and in the same year another revelation was
received by Smith, proclaiming him " seer, translator,
prophet, apostle of Jesus Christ, and elder of .the church."
Smith now began to baptize ; but, his character, which
was none of the best, being too well kno'mi in Fayette, he
found it convenient to remove with his followers, now
thirty in nvmiber, to Kirtland, Ohio, which was to be ■
the seat of the New Jerusalem. Here he had another
revelation, directing the saints to consecrate all their pro-
perty to God and to start a bank. This being done and
Smith appointed president of the bank, the country was
soon flooded with worthless notes, which fact, added to
other grievances, so enraged the neighbouring Christian
settlers that on the night of 22d May 1832 a number of
them dragged Smith and Rigdon from their beds and
tarred and feathered them. One year later, the church
was fairly organized, with three presidents. Smith, Rigdon,
and Frederick G. Williams, who were styled the first
presidency, and entrusted with the keys of Ihe latot
kingdom. About this time the licentiousness of Smith
might have led to the dissolution of the church but for the
accession of Brigham Young, a Vermont painter and glazier,
thirty years old, who turned up in Kirtland in 1 832, and was
immediately ordained elder. Yoimg's indomitaVie will, per-
suasive eloquence, executive abUity, shrewdness, and zeal
soon made their influence felt, and, when a further step W3,s
taken in 1835 towards the organization of a hierarchy by
the institution of the quorum of the " twelve apostles," who
were sent out as proselytizing missionaries among the " gen-
tiles," Young was ordained one of the " twelve " and d>j-
spatched to preach throughout the eastern States. In 18c j
a large temple was consecrated in Kirtland, and in the follow-
ing year Orson Hyde and Heber C. Kimball were sent off as
missionaries to England, where, among the labouring masses
in Manchester, Liverpool, Birmingham, Leeds, Glasgow,
and the mining districts of South Wales they achieved a
remarkable success. Early in 1838 the Kirtland bank
failed, and Smith and Rigdon fled to Caldwell county,
Missouri, where a large body of the saints, after having
been driven successively from Jackson and Clay countie."!,
had taken refuge and flourished. Smith's troubles, how-
ever, continued to increase. His gross profligacy had
repelled many of his leading supporters and bred internal
dissensions, whOe from the outside the brethren were
harassed and tireatened by the steadily growing hostility
of the native Missourians. To counteract the efforts of his .
enemies, a secret society was organized in Smith's favour
in October 1838, called the Danites, with the avowed
purpose of supporting Smith at all hazards, of upholding
the authority of his revelation and decrees as superior to
the laws of the land, and of helping him to get possession,
first of the State, then of the United States, and ultimately
of the world. To such a height did the inner dissensions
and the conflicts %rith the "gentiles" grow that they assumed
the proportions of a civil war, and necessitated the caUing
out of the State militia. Defying the legal officers. Smith
fortified the town and armed the saints, but finally had to
succumb to superior numbers. Smith and Rigdon were
arre-sted and imprisoned on a charge of treason, murder,
and felony, and their followers to the number of 15,000
crossed over into Illinois and settled near Commerce, Han-
cock county. Here they were shortly afterwards rejoined by
Smith, who succeeded in escaping from prison, and, having
obtained a charter, they founded the city of Nauvoo. Such
were the powers granted them by this charter as to render
the city practically independent of the State Government,
and to give Smith all but unlimited civil power. He
organized a military body called the Nauvoo legion, of
which he constituted himself commander with the title of
lieutenant-general, while he was also president of the
church and mayor of the city. On 6th April 1841 the
foundations of the new temple were laid, and the city
continued to grow rajfldly in prosperity and size. But
Smith's vices were beginning to bear fruit. Some years
previously he had prevailed on several women to cohabit
MORMONS
827
with bim, and in order to pacify his lavfol wife and silence
the objections of the saints he had a revelation on 12th
July 1843 expressly establishing and approving polygamy.
The proclamation of the new doctrine excited widespread
indignation, which found special expression in the pages
of the Expositor, a newspaper published by an old friend
of Smith, one Dr Foster. Smith at once caused the Ex-
positor printing-office to be razed and Foster expelled, on
which the latter procured a warrant for the arrest of Smith,
his brother Hyrum, and sixteen others. Smith resisted ;
the militia was called out ; the Mormons armed themselves ;
and a civil war seemed imminent, when the governor of
the State persuaded Smith to surrender and stand his trial.
Accordingly, on 27th June 1844 he and Hyrum were
imprisoned in Carthage jail ; but that same night a mob
broke into the prison and shot the two men dead. This
shooting was the most fortunate thing that had ever
happened to the Mormon cause, investing the murdered
president with the halo of martyrdom, and efifacLng public
recollection of his vices in the lustre of a glorious death.
Of the confusion that followed Smith's "taking off "Brigham
Voung profited by procuring his own election to the pre-
sidency by the council of the " twelve apostles," — a position
for which his splendid executive abilities well fitted him,
as subsequent events abimdantly proved. The following
year \vitnessed what appeared to be the culmination of
their misfortunes. The legislature of Illinois repealed
the charter of Nauvoo, and so critical did the situation
become that the leaders resolved to emigrate imme-
diately, and preparations were begun for 9, general exodus
westv/ard. Early in 1846 a large number of the body
met at Council Bluffs, Iowa, and those who had stayed
behind soon found cause to regret that they too had
not left Nauvoo, as in the September of the same year
that city was cannonaded, and the Mormons were driven
out. Meanwhile pioneers had been despatched to the
Great Salt Lake valley, Utah, and, their report proving
favouiable, a large body of emigrants was marched ^vith
military discipline across the wilderness to the valley,
where they immediately proceeded to found Salt Lake City,
and where on 24th July 1847 tboy were joined by their
chief, Brigham Young. In the May following the main
body of the saints set out to rejoin their brethren, and in
the autumn of that year reached Salt Lake City. Large
tracts of land were at once put under cultivation, a great
city sprang up as by magic, and the untiring industry,
energy, and zeal of the emigrants turned a barren wilder-
ness into a fertile and blooming garden. An emigration
fund was organized, missionaries were .■sent out, and soon
settlers began to pour in from all quarters of the globi,
particularly from Great Britain, Sweden and Norway, and
in less numbers from Germany, Switzerland, and France.
Strangely enough, and the fact deserves emphasis, Ireland
has furnished few if any recruits to the ra,use of Mormon-
ism. In March 1849 a convention was held at Salt Lake
City, and a State was organized under the name of Deseret,
meaning " the land of the honey-bee." A legislature was
also elected, and a constitution framed, which was sent on
to Washington. This Congress refused to recognize, and
by way of compromise for declining to admit the proposed
new State into the Union President Fillmore in 1850
organized the country occupied by the Mormons into the
Territory of Utah, with Brigham Young as governor.
District judges were also appointed by the Federal Govern-
ment ; but in 1851, a few months after their appointment,
they wera forced to leave by the aggressive tactics of
Young. Such bold defiance of the Federal Government
could not be ignored ; Brigham was suspended from the
governorship, and Colonel Steptoe of the United States
army appointed in his stead. The new governor, backed
by a battalion of soldiers, arrived in Utah in August 1854 ;
but so strong was the opposition which he met with that
he dared not assume oflice, and was forced to content him-
self with merely wintering in Salt Lake City, after which
he vrithdrew his troops to California. Nor did the other
civil officers appointed by the United States Government
at the same time show any bolder front. In February
1856 a band of armed Mormons broke into the court-
room of the United States district judge, and forced Judge
Drummond to adjourn his court sine die. His surrender
precipitated the flight of the other civil officers, and with
the sole exception of the United States Indian agent they
withdrew from Salt Lake City. These facts led President
Buchanan to appoint a new governor in the person of
Alfred Gumming, the superintendent of Indian affairs on
the upper Missouri, who in 1857 went to Utah, accom-
panied by Judge Eckels of Indiana as chief justice, and
by a force of 2500 soldiers. Enraged by this aggressive
action, Brigham Young boldly called the saints to arms.
In September the United States army reached Utah, but
on 5th and 6th October a band of mounted Mormons
destroyed a number of its supply trains, and a few days
later cut off 800 oxen from its rear and drove them into
Salt Lake City. The result was that the United States
army, now commanded by Colonel A. S. Johnston, was
compelled — it being now mid-November— to go into winter
quarters at Black's Forks, near Fort Bridger. In the
game year a party of Mormons and Indians, instigated
and led by a Mormon bishop named John D. Lee, attacked
a train of 150 non-Mormon emigrants at Mountain Mea-
dows, near Utah, and massacred every souL Governor
Gumming at once declared the Territory in a state of
rebellion; but in the spring of 1858, through the inter-
vention of Thomas L. Kane of Pennsylvania, armed with
letters of authority from President Buchanan, the Mormons
were induced to submit to the Federal authoritj-, and
accepted a free offer of pardon made to them by the United
States Government as the condition of their submission.
Matters being thus settled, the Federal troops encamped
on the western shore of Lake Utah, some 40 miles from
Salt Lake City, where they remained until withdrawn from
the Territory in 1860. On the close of the American Civil
War a Federal governor was again appointed, and in 1871
polygamy was declared to be a criminal offence, anci Brigham
Young was arrested. This action, however, on the part of
the United States Government was merely spasmodic, and
the Mormons continued to practise polygamy, and to increase
in wealth and numbers until 29th August 1877, when
Brigham Young died, leaving a fortune of 82,000,000
(£400,000)to 17 wives and 56 children. He was succeeded
in office by John Taylor, an Englishman, although the
actual leadership fell to George Q. Cannon, "first coun-
sellor " to the president, and one of the ablest men in the
sect. The year 1877 was otherwise signalized in Mormon
history by the trial, conviction, and execution of John D.
Lee for the Mountain Valley massacre of 1857. Of late
years the question of Mormonism has largely occupied
public attention. In 1873 Mr Frelinghuysen introduced
a bill severely censiuing polygamy, and declaring that the
wives of polygamists could claim relief by aotion for divorce.
In 1874 the committee of the House of Representatives
reported a bill which reduced Utah to the position of a
province, placing the control of affairs in the hands of
Federal officials, and practically abolishing polygamy. In
the same year George Q. Cannon was elected a delegate
from Utah, and though his election was contested it was
confirmed by the House of Representatives. This decision,
however, was accompanied by the passing of a resolution
by a vote of 127 to 51, appointing a committee of investiga-
tion into Delegate Cannon's alleged polygamy, — he having,
•328
M O R — M O R
it was asserted, four wives. Later in the same year tbe
Utah Judiciary Bill, attacking the very foundation of
Mormonism, passed the House in spite of the eloquent
opposition of Cannon. Other steps in the same direction
have since been taken, and bills passed, having for their
object the extirpation of polygamy, but all without imme-
diate and practical effect. It is, however, a question of
time merely ; polygamy is doomed. The secessioti, chiefly
because of his opposition to the practice, of Brigham
Young's son, a Christian preacher, and of a large body
of other anti-polygamists who claim to be the true Latter-
Day Saints, represents not an individual opinion but the
deep-rooted conviction of a great party, and the day is not
far distant when the Mormons who acknowledge John
Taylor as chief prophet must consent to lop off polygamy
or cease to exist as a corporate body of the United States.
Already there are not wanting signs of approaching dis-
solution, of which perhaps the most significant is the con-
ference of the "Reorganized Church of Jesus Christ of Latter-
Day Saints," held on 6th April 1883, at Kirtland, Lake
county, Ohio. This sect originated in 1851, seven years
after the death of Joseph Smith, when several ofiicers of the
church met and claimed to have received a revelation from
God, directing them to repudiate Brigham Young, as not
being the divinely-appointed and legitimate successor of
Joseph Smith, and as being the promulgator of such false
doctrines as polygamy, Adam-God worship, and the right to
shed the blood of apostates. Nothing of special importance
occurred, however, until 1860, when Joseph Smith jun.,
the eldest son of the founder of the faith, became identi-
fied with the Reorganized Church as its president. Since
then the seceders have prosecuted missionary work through-
out the United States, Great Britain, Canada, Scandinavia,
Switzerland, Australia, and the Society Islands, until their
communicants are said to pumber over 27,000. Their
headquarters are at Piano, Illinois, to which place they
removed from Lamoni, Iowa, in 1881. The Reorganized
Church holds that the legitimate successor to Joseph Smith
was his eldest son, that the allegation that Smith intro-
duced polygamy on the strength of divine revelation was
an invention of Brigham Young, that the Utah Church
has departed grievously from the faith and practices laid
down in the Book of Mormon and subsequent revelations
to Joseph Smith, and that the Reorganized Church is the
only true and lawful continuation of, and successor to, the
original church, and as such is legally entitled to all that
chtirch's property and rights. And it was to celebrate the
decision of the United States Court of Ohio confirming
this last claim, and vesting in them the right to the temple
consecrated in Kirtland, Ohio, in 1836, and for nearly forty
years disused owing to litigation, that the Reorganized
Church met in that temple on the 6th of April 1883.
Returning to the main body, it may be added that the
population of Utah is 147,000, of whom 123,000 are
Mormons ; but as the saints are scattered over the globe
it is difficult to arrive at a just estimate of their complete
numerical strength. In Idaho, Arizona, Washington,
Colorado, Montana, and Wyoming they have of late years
made great progress, and their number in the United
States outside of Utah cannot fall much under 27,000.
In Europe they have also many adherents, and a careful
study, based on recent official statistics, would place their
entire number at 213,000.
Qovemmeni, — At the head of the body is a president, who pos-
MBSes Bupreme authority, supported by two couuBcllors. Tncso
three are supposed to be the successors of Peter, James, and John,
and constitute what ia known as the "first presidency." Then comes
the " patriarch," whose chief duty is to bless and lay on hands, and
aft«r him the " twelve apostles," forminj^ a travelling high council,
and receiving a salaiy of $1500 a year each. Of these the president
ia a officio one, ard endowed with authority equal to the other
eleven. Their dnties are important They ordain all other cfficera,
elders, priests, teachers, and deacons, lead all religious meetings,
and administer the rites of baptism and sacrament. Fourth coma
the seven presidents of the "seventies," each body comprising seventy
elders ; there are eighty seventies in Utah, each of which has seven
presidents, and every seven one president. These seventies maks
annual reports, and are the missionaries and propagandists of the
body. Fifth come the "high priesti," whose chief duty is to officiate
in all the offices of the church in the absence of any higher autho-
rities. After them comes the presiding bishop, who superintends
the collection of tithes, which amount to ?1, 100, 000 annually. The
church is mado up of 23 stakes, each having a president, and ia
divided into wards, which are subdivided into districts, each of
which has a certain number of teachers, a meeting-house, Sunday
school, day school, and dramatic, debating, and literary societies.
Dodrine, — The Mormons no longer claim to be a Christian sect,
any more than do the Mohammedans. A system of polytheism has
been grafted on the original creed, according to which there are
grades among the gods, the place of Supreme Kuler of all being
taken by the primeval Adam of Genesis, who is the deity highest
in spiritual rank, while Christ, Mohammed, Joseph Smith, and
Brigham Young also partake of divinity. The business of these
deities is the propagation of souls to people bodies begotten on
earth, and the sexual relation permeates every portion of the creed
as thoroughly as it did that of ancient India or Egypt. The saints
on leaving this world are deified, and their glory is in proportion
to the number of their wives and children, — hence, the necessity
and justification of polygamy, and the practice of having many
wives sealed to one saint. Their distinguishing points of faith
are : — religiously, a belief in a continual ^vine revelation through
the inspired medium of the prophet at the head of the church ;
morally, polygamy, though this is expressly condemned in the
Book of Mormon^ and was grafted on the original faith by Smith ;
and, socially, a complete hierarchical organization. They believe in
the Bible as supplemented by the Book of Momion and the Book of
Doctri-iie ; in the gift of prophecy, miracles, and casting out devils ;
in the-imminent approach of the end of the world ; m their own
identity with the apocalyptic saints who shall reign with Christ in a
temporal kingdom, either in Missoiui or Utah ; in the literal
resurrection of the body ; in absolute liberty of private judgment
in religious matters ; and in the salvation of a man only if he believes
in Christ's atonement, repents, is baptized by immersion by a.
Christ-appointed apostle, and receives the laying on of hands for
the gift of the Holy Ghost by duly authorized apostles. Amon^
their minor niles as laid down in A Word of Wisdom, supposed t.i
have been revealed to Joseph Smith, 27th February 1833, are these
recommendarions : — that it is not good to drink wine or strong drink,
except at the Lord's Supper (and even then it should be home-made
grape-wine), or to use hot dnnks or tobacco, — the former being meant
for the washing of the body, and the latter for the healing of bruises
and sick cattle ; man's proper food is herbs and fruit, that fi>r
beasts and fowls, grain ; and, except in winter and in case of famine
and severe cold, flesh should not be eaten by man. Infant baptisri
is also condemned, but the children of -the saints who have reached
their eighth year should be baptized. The deceased, also, can be
baptized by proxy, and in this way "Washington, Franklin, and
others have been vicariously baptized into the church.
See BooS: o/Afofmon (1879) ; Boojto/Doc(nnc and Covenan(s(1870); John Hyde
Jon., Jlfomonism, iU Leadsn and Dnigns (1S57): B. G Ferris, VIoh and IH
Mormons (1854); N. W. Green, ilomonxsm (1870): T. B. H. Stenhouse, Fock^f
Mountain Sainls(lSTi); H. Mayhcw, TAe Jl/oraoiu ; Elder Jolin Jaques, Cii«-
'chtnt /or Children (1877) ; John W. QDnnison, ilomwns, or Lalttr-Day Saintt
(18J.2): Hepworth Dixon, Spiritual Wives (1868); J. H. Beadle. Ll/e in Utah
(1870). (J. FK.)
MORNAY, Philippk db (1549-1623), Seigneur du Ples-
sis-Marly, very generally known as Mornay Du Plessis or
Du Plessis-Momay, one of the most distinguished members
of the Protestant party in France, was bom at Buhy in
Normandy on 5th November 1549. As a younger son
be was destined for the church, and with this view was
sent to the OUige de Lisieux in Paris, but in' his eleventh
year, along with the rest of his family, he abandoned
Roman Catholicism, continuing, however, with zeal and
success his studies not only in classical and general litera-
ture but also in theology. In the autumn of 1567, on the
outbreak of the second religious war, he joined the army
of Cond^, but waS prevented from taking an active part
in the campaign by a fall from his horse, which broke his
leg. In the following year he went abroad, and, after
spending the winter at Heidelberg, travelled extensively
in Italy, Germany, the Low Countries, and England,
learning the languages and acquiring the friendship of
many of the distinguished men of all these countries. In
M O R— M O R
829
June 1672 he returned to France, and had begun to enter
npon a diplomatic career (his earliest extant " m^moire."
laid by Coligny before Charles IX., had reference to the
duty of France to support the Low Countries in their
struggle for independence) when the St Bartholomew mas-
sacre, from which he escaped with difficulty, compelled
him to take refuge across the Channel. There he rendered
valuable services to William of Orange, and also to the
duke of Alen^on-Anjou, as a serai-official political agent.
Ketuming to France at the instance of La Noue towards
the end of 1573, he took part with various success in
numerous military enterprises, and was made prisoner at
Dormans in 157 5 (10th October), but not having been re-
cognized he got oft" for a small ransom. Shortly afterwards
he married Charlotte Arbaleste at Sedan, and at her re-
quest wrote as a bridal present the Disamrs de la Vie et
de la Mort (1576), which has been so often reprinted and
translated. In 1577 Henry of Navarre made him a mem-
ber of his council and sent him on a diplomatic mission to
England, and during this visit, which lasted more than a
year, he found time among his other pressing occupations
to prepare for the press his Traite de r£glisi oh Von traite
des principaies qvestions qui ont He mues sur ce point en
nostre temps (1578), which at once became popular. From
July 1578 till his return to France in 1582 he was chiefly
in the Low Countries, engaged in public business, and
VJuring this interval he wrote and published a considerable
work in apologetical theology {Traite de la write de la
religion chretienne contre lef Alhies, £picuriens, Payens,
Juifs, etc., 1581). With the death of the dvike of Anjou
in 1584, by which Henry of Navarre waa brought within
sight of the throne of France, the period of Momay's
greatest political activity began ; his importance in the
Huguenot counseb was further increased in 1588 by the
death of the prince of Cond^, to whose influence he practi-
cally succeeded. In April 1589 he was re^varded for the
reconciliation of the two Henries with the governorship of
Saumur, and he took active part in many of the military
operations that followed the assassination of Henry III.
in the following August. He was present at the siege of
Dieppe, fought by the side of Henry IV. at Ivry, and was
one of the besiegers of Rouen in 1591-92, until sent on a
mission to the court of Elizabeth. A crisis in Ms political
career was marked by Henry's abjuration of Protest-
antism in July 1593, which gradually led to Momay's
withdrawal from the court. In this year it was that he
founded the Protestant academy or university of Saumur,
which had a distinguished history until its suppression by
Louis XrV. in 1683. In 1598 he published a work on
which he had long been engaged, entitled De Vinstitution,
usage, et doctrine du saint sacrement de PEucharistie en
V£glise ancienne. It having reached his ears that Cardinal
Du Perron had alleged that of the (thousands of) citations
in thii controversial work he could point out five hundred
that were falsified or misunderstood, he challenged his
assailant to a public discussion. This was at last arranged
for by the good offices of the king, and took place at
Fontainebleau on 4th May 1600. Only nine passages
were discussed, but in each case the decision, one is not
surprised in the circumstances to learn, went against the
Protestant. Mornay, from whom every indication of the
particular passages to be impugned had been persistently
■nithheld, was forced by supervening illness to withdraw.
Only once again did he appear at court, in 1607. He
continued, however, to give his party the benefit of his
counsel and active support to the end of his long and busy
life. His last work, entitled Mystire d'iniquite, c'est it
dire, FAistoire de la Papaute, appeared in 1611. In 1618
he was chosen a deputy to represent the French Protest-
anU at the synod of Dort. ■Prohibited by Louis yTTT |
from personally attending, he nevertheless contributed
materially to the deliberations of that assembly by written
communications. In 1621 he was deprived of his governor-
ship ; and his death took place at La For^t-sur-Sivre on
11th November 1623.
Two volumes of iUmoires, from 1572 to 1589, appeared at L«
For^t in 1624, and a continuation, in two volumes, at Amsterdam
in 1652 ; a more complete edition (Mimoircs. corrcspondnnus, ct vie)
in twelve volumes, 8vo, was published at Paris in 1624-25. The
greater number of hia works were translated into English during
his lifetime.
MORNT, Chaelis Auouste Loms Joseph, Duo de
(1811-1865), was the natural son of Hortense Beauharnais,
queen of Holland, and of the comte de Flahaut, a leading
dandy of the period, and was thus brother to Napoleon
in. The secret of his birth (23d October 1811) was care-
fully kept ; he was acknowledged as son by the comte de
Morny for ■& consideration, and was brought up by his
paternal grandmother, Madame de Souza, a writer of
society novels, and a woman of great wit and high breeding.
As a boy of nineteen he was declared after the revolution
of 1830 a hero ot July, and was entered at the staff college.
In 1832 he was gazetted suVlieutenaut, and served in
Algeria as aide-de-camp to General Oudinot ; he was pre-
sent at Mascara and Constantine, and was made a chevalier
of the Legion of Honour. In 1838 he returned to Paris,
and began his career as dandy and speculator. In the
first capacity he set the fashions both of dress and manners
to the young men of Paris, and conceived the idea of the
modem society journal, and in the second established a
manufactory of beetroot sugar at Clermont-Ferrand. This
last idea brought about his election for the department of
the Puy-de-D6me. In the chamber he voted consistently
with the ministers. The republic of 1848 marked the
crisis in his fortunes, and by 1851 all his speculations had
failed, and aU his property was sold. In desperation he
determined to play a part in politics, and was the heart
sind soul of the coup cTetat of December 1851. The success
of the coup cTetai was certain, owing to the fear of the
extreme republicans entertained by the great majority of
the nation, and all that was needed was a head for intrigue
and an utter absence of scruples to shed innocent blood.
Morny and St Arnaud fulfilled these requisites. Moray
was on the day of the coup d'etat made minister of the
interior, but he had no taste for the drudgery of adminis-
tration, and in January 1852 found an excuse for resigning
on the question of the property of the Orleanist princes.
The empire established, he was again able to begin specu-
lating, and used both the money of the state and his
influence with his brother for the success of his schemes.
He had been in 1852 re-elected deputy for Clermont-
Ferrand, and waa in 1854 elected president of the corps
legislatif, an office which he held for the rest of his life.
This office in every way suited him ; he had large pay,
and resided in a magnificent official residence, where he
produced little plays to admiring audiences. The work
was not hard, being chiefly to maintain the Government
majority in a good humour by sumptuous entertainments,
and to win over the Liberals by the same tactics. He still
speculated in railways, pictures, mines, and even in a new
watering-place, Deauville, and, being absolutely unscru-
pulous and venal, amassed an immense fortune in spite
of the utmost extravagance. In 1856 he was special
ambassador at the coronation of Czar Alexander EL, when
he spent immense sums, and married a wealthy Russian,
Princess Troubetzkoy. In 1862 he was created a duke,
and in 1865, after continuing to the last his career of dissi-
pation, died of sheer anaemia from the measures he took
to keep himself fit for yet further excesses.
OC the due de Morny little good can be said either aa a statesman
or a "">", He looked upon everything from a purely selfish point
830
M O R — M O R
fWet.
of view, at^X would not have denied it ; but lie was shrewd enough
to perceive that the empiro rested on the prestige it maintained for
France not only in war but in fashion, and in assisting the empress
to make Paris the centre of fasliion for the whole civilized world he
knew he was not only pleasing himself but doing a service to tlic
empire. He was a thorough man of the world, and was witty as
such, but the wit does not appear at its brightest in his plays,
published under the name of Saint-Remy, of which perhaps the
most readable is M. Choujlcui-y rcstcrn chcz lui. He had great
influence over tlie emperor, but could lay no claim to personal
fidelity, as could his less able but equally unscrupulous colleague,
M. de Persiguy.
.For his life consult H. CastiUe. .V. lic Monty, 1S59, and De la Gueronuicre,
A(udcSf(jw7J(ra(W/)o/i7(7ifes(lS5Li);nIsoAlton-Shee's.fl/<7JW)ires(lS6S-G9). His char-
acter is adiiiiiably alcetcliej as tlie due de Mora ia A. Daudcfs novel Le Kabah.
MORO, Attoxi (c. 1512-1581), otherwise known as
SiK Anthoxy More, an eminent portrait-painter, was born
at Utreclit, in 1512 according to some, but in 1525
according to Van JIander in his Ilei Leven der Schild<rs.
He studied his art under Jan Schoorel ; and after making
a professional visit to Italy he commenced to paint por-
traits in the style of Hans Holbein. His rise to eminence
was rapid. In 1552 he was invited to Madrid by tlie
emperor Charles V. to execute a likeness of Prince Philip.
Two years afterwards he was in London painting the
portrait of Queen Mary. For this picture an annual
salary and, as some suppose, tlie honour of knighthood
were conferred upon him. He was also employed to
sketch the likenesses of several of the English nobility.
On the death of Mary in 1558 Moro returned to Spain,
and lived there for two years in great honour with Philip
II., executing, in addition to portraits, several copies after
Titian. Having compromised himself with the Inquisition,
he repaired to the Netherlands and was received into the
service of the duke of Alva. His death took place at
Antwerp about 1581. Among his figure-pictures Van
•Mander specifies the Circumcision of Christ, executed
for Antwerp cathedral, as one of the most notable. His
portraits are full of individuality, and characterized by
firm and solid rendering of flesh. Several admirable
examples are preserved in Madrid ; among the rest the
portrait of Queen JIary of England, .which has been
excellently etched by Milius {L'Art, 8th December 1878).
" Moro's style," says Stanley in his Dutch and Flemish
Painters, "so much resembles that of Holbein as to fre-
quently create a doubt to ^vhich of them a portrait is to
be attributed ; but he is not so clear and delicate in his
colouring (perhaps from having painted so much in Spain)
as that master."
MOROCCO, or JI.^ROcco, the terra (corrupted from the
name of the city JNIarrAkush) used in English to designate
the Maghrib al-AksA or extreme west of the Arabs, is the
country at the north-western corner of the African continent,
with the Jlediterranean on the north and the Atlantic on the
west. Its landward limits can only be vaguely defined. The
eastern frontier towards Algeria, determined by the treaty
of 1844, is a purely conventional line starting from the
mouth of a small stream called the Skis and running across
country in a general south -south -east direction. The
southern boundaries expand and contract according to the
power and activity of the central authorities. Behm and
Wagner (1882), who include Tafilelt, Kenatsa, Figig, Twat,
Gurara, Tidikelt, the plateau of Tedmaid, etc.. estimate the
total area of the sultanate at 305,548 square miles ; and this,
which is about twice the size of Algeria, or five times that
ef England and Wales, may be taken as a maximum. The
allegiance of many of the tribes within this compass is
que3tiono,ble and intermittent. Morocco is still the portion
of Northern Africa about which European information is
most defective, and the ordinary maps are composed to a
large extent of most unscientific material eked out by
probabilities and conjecture. Since the middle of the
present centmy a good deal has been done in >he way of
exploration, mainly in the lowlands and steppes sloping
towards the Atlantic — the country of the great historical
cities of Tangiers, Fez, Meknes (Mequin,cz), and Morocco ;
but even there what lies but a fejv miles east or west of
some track traversed by Europeans for centuries remains
matter of question.
Since the publication of Arlett's survey from Cape
Spartel to Cape Bojador (1840-44) and of Vincendon-
Dumoulin and Kerhallet's surveys from the Strait of Gib-
raltar to the Algerian frontier (1853-57) the seaward aspect
of Morocco has been known in detail. To the Mediter-
ranean it presents for a distance of about 200 miles the
rugged profile of the Rif hills (still unexplored), which
generally end in lines of cliff broken at intervals by narrow
sweeps of sandy beach,' but occasionally open up into beau-
tiful and fertile valleys, with abundant evidence of human
occupancy and tillage. About 6 miles west of the Skisj
lies the mouth of the great river Muliiya ; and 10 miles
farther 'on, opposite Cape del Agua (Ras Sidi Beshir), is
a group of dry and barren islands known as the Zafarines,
which form the best roadstead on the Rif coast.^ Be-
tween Point Quiviana and Melilla runs a low and sandy
shore in front of a great salt marsh, the Puerto Nuevo of
the Spaniards. Melilla (Malila) is a fortified town, held
by the Spaniards since 1653, built on a rocky peninsula
and connected by lines of rampart with Fort Rosario on
the heights behind. Near the village of Azaiien is a wide
open shore with the only sand-dunes on all this coast.
The fine semicircular bay of Alhucemas is the seaward
end of one of the most beautiful valleys in the Rif, clothed
with verdure and dotted with hamlets. A Spanish presidio
occupies one of the larger of the Alhucemas islands (Al-
Mazemma), which are identified with the Ad Sex Insulas
of the itineraries. Another Spanish fortress crowns the
rocky island of San Antonio or Penon de Velez ; and in
the valley oflF which it lies stood a town known to the
Spaniards as Velez de Gomera, to the Arabs as BAdis, which
continued to be a place of importance in the 16th centmy.
The so-called Bay of Tetuan (Tettiwin) — the town is just
visible from the sea — is little more than the straight stretch
of coast between Cape Mazari on the south and Cape Negro
or Negrete on the north ; but the prominence of these two
headlands gives it an appearance of depth. From Cape
Negi-o northwards to Ceuta the most notable object on
the horizon is the summit of Jebel Jliisil, which, though
situated on the Strait of Gibraltar, towers above the inter-
vening hills. Ceuta (Sebta), the most important and
flourishing of the Spanish settlements in Jlorocco, occupies
a peninsula, — the head, Mt. Acho, standing about 1 miles
out to sea, and the neck being low and narrow. It marks
the eastern end of the strait. Westwards, the first point
of interest is again Jebel MusA, the Elephas of Strabo, and
the Apes' Hill of Englisli charts ; the truncated top is
usually hid in clouds. About 20 miles farther along the
coast lies the Bay of Tangiers (Tanja), by far the finest
harbour in Morocco. West from Tangiers runs the Jebel
Kebir (880 feet at its highest), the seaward extremity of
which forms the celebrated Cape Spattel, the north-west
angle of the African continent, known to the ancients as
Ampelusia or Cotes Promontorium. The lighthouse, built
in 18G4 at the cost of the sultan of Jlorocco, and main-
tained at the joint expense of England, France, Italy^ and
Spain, is the only one on tlie western coast.
The Atlantic coast of Morocco is remarkable for its
regxilarity and sameness ; not a single gulf or noteworthy
estuary occurs throughout its whole length ; the capes
^ The uaiiie is derived from the Arab tri^-c of the Beui Ja'far, *vlio
settled on the neighbouring mainland at \'''. conouest. Since ISJS
the islands have belonged to Spain. They fi: i.'«u'-ified with the Ai»
Tres Insulas of the Roman itineraries.
MOROCCO
831
ore few and for the most part feebly maxked. South-
ward from Cape Spartel the shore sinks rapidly till it is
within a few feet of the searleveL In the low cUflf which
it forms about 4J miles from the lighthouse there is a
great (juarry, which from remote antiquity has yielded the
hand-mills used in the Tsingiers district. A stretch of
low marshy ground along the Tahaddart — the estuary of
the W4di Keblr (W. Muharhar) and W. al-Khamib — agrees
with ScyWs Gulf of Cotes (Tissot). Three or four miles
farther south lie the ruins of the town of Nebrosh, built by
Moors from Andalusia ; and 4 or 5 miles more bring us to
AkUA or Arzilla, the ancient, Colonia Julia Constantia Zilis
or Zeles. Since its bombardmeut by the Austrians in 1829
it has been a wretched little place, with a mixed Moorish
and Jewish population of about 1200.^ For the next 16
miles, between AtOA and Larash or El-Araish (q.v.) the
coast has a tolerably bold background of liills, Jebel Sarsar
near Fez forming an important landmark for the latter town,
which, with its Phoenieian, Koman, and mediaeval remains,
is historically one of the most interesting places in Morocco.
A line of reddish cliffs about 300 feet high runs south
for about 10 miles from the W. Aulkos, at whose mouth
the town is built ; then the coast sinks till it reaches MilU
Bd Selham, an eminence 220 feet high. Between MiilA
Bii Selham (often wrongly called Old Mamura or Marmore)
and a similar height crowned by the tomb of Sidi "Abd
Allah Jelill lies the outlet of the Blue Lake (Marja Zarkd),
10 or 12 miles long. Farther south, and separated from
the sea by an unbroken line of rounded hills (230-260
feet), is the much more extensive lagoon of Ras al-Dura,
which in the dry season becomes a series of marshy meres,
but in the rainy season fills up and discharges into the
Sebii. Eastward it is connected with the Marjat al-Gharb,
fed by the W. Meda. On the south side of the outlet of
the Sebil lies Ma'miira, probably foimded by 'Abd al-
Mumen, and originally named Mahdfya, after the Almohade
Mahdl Twenty miles farther is the mouth of the Bii
Rakrak, with its cluster of interesting towns : Sallee (SaUt)
on the north side, long famous for its piracies and still one
of the most fanatical places in the empire, and on the south
side New Sallee (Habit) with its conspicuous tower of
Hasan, and Sheila (Sella of Leo Africanus) with its inter-
esting ruins. Onward for 100 miles to Point Azammtir
and the mouth of the Umm Rabf river a line of hills skirts
the sea ; the shore is for the most part low, and, with the
exception of capes at Fadila (a small village) and DAr al-
Baid& or Casa Blanca, it runs in a straight line west-south-
west. Casa Blanca, the ancient Anfd, once a flourishing
port,, was ruined by the Portuguese (1468) in revenge for
ita piracies. It is now a place of 4000 inhabitants, and
has a thriving export trade in maize, beans, and wool,
and a European colony of about 100 persons. Azammur
(that is, in Berber, " The Olives," viz., of the Sheikh Bii
Shuaib), with 1000 inhabitants dependent on the shebbel
fisheries in the river, stands on an eminence about IJ
miles from the sea on the south side of the Umm Rabi'.
The bay of Mazagan (MAzlghan), a few mOes to the south,
curves westward with a boldness of sweep unusual on this
coast. The town of Mazagan was founded by the Portu-
guese in 1506, and held by them till 1769.^ About 8
miles to the south and less than a mile inland lie the
extensive ruins of Tit, a town which proved a thorn in
the side of the people of Mazagan till they sallied forth
' The absurd story that about the 9th century it was an English
possession has its root in the visits of the Normans to this quarter.
The modem town sprang from a fortress built to protect the coast
against them (Dozy, Recherches, 3d ed., ii. 264 sq.).
' The Portuguese settlers, who had to leave it when Don Jos^ decided
on surrendering this last stronghold of his conntryin Morocco, were after-
vaids sent to Brazil, where they founded Villa Nova de Mazagan.
and destroyed it. At Capo Blanc (so called from its
white cliffs) the coast, which bulged out at Cape Mazagan,
again bends east to resume much the same general
direction for 55 miles to Cape Can tin. On this stretch
the only point of interest is Walidiya, formerly Al-Ghait ;
the excellent harbour praised by Edrisi is formed by an
extensive lagoon, and M. Tissot thinks that by a little
dredging the place would again become the safest ship-
ping station on the whole Morocco seaboard.^ Beyond
Cape Cantin (300 feet high) the coast becomes bolder and
more iiTegular, especially after the mouth of the Tenslft is
passed. About 18 miles farther lies Saffi (Asfi), "by far
the most picturesque spot on the west coast," with the high
walls and square towers of its Portuguese fortifications
shown to advantage by the ruggedness of the site. South
of MooADOE(2.y.),and onwards beyond the limits of Morocco,
the coast, becoming ever more and more inaccessible and
dangerous in winter, is emphatically known as the Iron
Coast. From Cape Sim or Ossim (Ras Tagriwalt), 10 miles
south of Mogador, the direction is due south to Cape Gir
(Igir Ufrani),- the termination of Jebel Ida u Tanan (Rabbi
Mardoch^e), the last spur of the Atlas proper. Rounding
this headland we reach Agadir (Agadir 'n Igir), the Santa
Cruz Major or Santa Cruz de Berberia of the Spaniards,
formerly knovni a? the Gate of the Soudan.* It is a little
town with white battlements three-quarters of a mile in
circumference, on a steep eminence 600 feet high. In
the 15th century it was seized by the Portuguese, and
Don Manuel caused it to be fortified ; but in 1536 it
was captxured by Muley (Maul4i) Ahmed al-Hasan. Its
merchants were removed'to Mogador in 1773. At the
mouth of the Siis Leo places three little towns called Messa
(Mdssa), with a mosque popularly reputed the scene of
Jonah's restoration to terra firma. The port of this name,'
regularly visited by the Genoese traders in the 1 6th century,
who exported skins, gum, wax, gold, and indigo, is no doubt
at the mouth of the W. Mdssa, 20 miles farther south.'
Ifni, situated in 29° 23' N. lat., and Sidi Worzek, the Cape
Non ' of the Portuguese, are the only points calling for
notice till the better known Cape Nun is reached, which lies
5 or 6 miles north of the W. D4r'a. With the Der'a the
Sahara may be said to begin.
On most maps the interior of Morocco is represented as
extremely mountainous j but, while it is traversed from ea|t
to west by more than one strongly-defined range,"the greater
part of the surface is really occupied by undulating steppe-
Uke tracts diversified by low hills. The backbone of ^e
coimtry is the Great Atlas (Daran of the Berbers).^ At
its western extremity the range averages "from 4000 to
5000 feet in height ; after a slight falling off for a few
miles it rises till it attains an elevation of 10,000 feet;
beyond the pass (about 60 miles from the sea) which leads
from Morocco to T.ir>idant the siunmits seem to be between
11,000 and 11,500 feet; about 40 miles farther east there
is a second pass at an altitude of about 7000 feet ; and
beyond that the main ridge continues 30 miles at a height
of about 12,000 feet, with a few peaks reaching to 13,000
or 13,500 feet. Snow lies on some of the summits as late
' Bull, de la Sac de Ologr., Paris, 1875.
* This must not be confomided with Santa Cruz de Mar Pequefia,
a post established in 1476 somewhere on this coast by Herrera, lord
of the Canary Islands, and in modem times the subject of much geo-
graphical disputation. After obtaining permission to reoccupy the
site the Spanish Government was unable to identify it.
' See Valentin Ferdin.and, Bcschreibung West Afrika^s (Uem. of
the Acad, of Munich, 3d Class, pt viii. ;.
• Ya'kiiM, Descr. al-Maghribi, p. 126 ; Etst des Scrbhes, ii. 279.
' No, Non, Nor, Naum, Nao, are among the vaiious readings. It
was another Cape Kon to the south of Cape Bojador which seems to
have given rise to the proverb, Qiiem pasar o cabo de Xao ou toniara,
on ndo. See Bol. de la Soc. Geogr., p. 316, Madrid, 1880.
8 Pliny says the natives called the Atlas "DjTin."
832
MOROCCO
as Juue, but it is probable that none of them retain it
throughout the year. Taken as a whole, the Atlas has a
mean elevation higher than that of any other range of
equal length in Europe or in the African and Asiatic
countries bordering on the Mediterranean. From the
lowlands to the north it has a very fine appearance, rising,
as it seems, in steep and almost abrupt ascent, though the
real distance from foot to summit is a slope ot 15 miles
(compare the panorama prefixed to Hooker and Ball's
Morocco).
"What is the culminating pointof the range is quite unkno^ii; the
Miltsin peak has no claim to that distinction. The English embassy
of 1829-1830 advanced up the northern slope only a little beyond
Tasseremut (3534 feet), and Davidson in 1836 merely reached the
town, and then turned westwards. From Tasseremut eastwards the
range is altogether unexplored for 200 miles till we come to the
route followed by Ahmed b. Hasan al-Mtuvi (1789), Caillie (1827),
and Rohlfs (1863). 'The English expedition of 1871 (Hooker and
Ball, &c. ), besides visiting Tasseremut, went up the Urika valley to
a height of 4000 feet, up the Ait Mesan valley to the Tagherot pass
(11,484), and up the Amsziz valley to the summit of Jebcl Tezah
(11,972 feet). In the Tagherot pass Mr Maw was the only one of
the party who reached the waterslied ; but from Jebcl Tezah a good
view was obtained southward across the great valley of the Sus to
the Anti-Atlas, which appeared to be from 9000 to 10,000 feet high.
In 1880 Dr Lcnz crossed the range by the ordinary route from
lloiocco toT.'inidant. " First," he says, "is a chain of comparatively
low and fiat hills consisting of Cretaceous and Tertiary rocks ; then
follows a plateau with ranges of red, probably Triassic, sandstone ;
and finally come the higher and steeper peaks of clay slate with
great metalliferous deposits. The pass whore the descent towards
Siis begins is called Bibauan, and lies 4000 fee^ above the sea. The
route down to ' Emnislah ' is steep, difficult, and at times dangerous. "
As to the relation of the An-ti-Atlas to the Atlas proper at its
western end nothing certain is known..
All the principal rivers of Morocco take their rise in the
Atlas mountains, and the headwaters of the Muliiya, the
Sebii, the Umm Rabi', the Der'a, and the Zlz are all to
be placed in that part of the range which lies between
32° 20' and 32° 30' N. lat., and between 3° 30' and 5° W.
long. In almost every instance the summer current is
comparatively feeble, but the wide beds and often high
steep banks are sufficient of themselves to show the change
produced by the rains of winter and the thaws of spring.
The JIuluya (^lulucha and-Malva of Pliny, <tc.) is mainly
interesting as the river which the French have long wished
to make the western boundary of Algeria. Its course is
almost entirely luiexplored. About 34° 20' N. lat. Captain
Colvile found it some 200 yards wide but quite shallow ;
al-iout 25 miles east of its source where it is crossed by the
route to Ziz it is already a powerful stream with a deep
bed cut in the granite rock, and shortly afterwards it is.
joined by the W. Sgimmel, a still larger affluent (Rohlf.s).
Of the lesser sti-eanis which flow into the Mediterranean it
is enough to mention the W. JIartil or Martin (otherwise
jW. Bu Sfiha, W lias, W. Jlejeksa), which falls into the
iBay of Tetuan, and is identified with the Tamuda of
Pliny and Tlialuda of Ptolemy. On the Atlantic seaboard
'north of the Sebii there are a number of comparatively small
streams, the chief of which is the very winding W. Aulkos
or Lokkos, with several tributaries. If Renou's statement
that theSebu (the Subur maynifictts et navigabilis oi Pliny)
had a course not much inferior to that of the Seine be
somewhat of an exaggeration, it may at least be compared
to the Thames in length and width, though not in steadiness
and depth of current. At Meshra'at al-Ksiri, about 70
imiles from its mouth, it is about 10 feet deep in the month
'of May and more than 4C0 feet wide ; and, though its
Ibanks are 21 feet high, extensive inimdations occur from
'time to time. The tide ascends as far as Al-Kantara, 15
I miles above Ma'mi'ira, and steam barges with a small draught
[of water could make their way to the ford just mentioned,
[and possibly even as far as Fez (Trotter). Affluents of the
ISebi'i are W. Mikkes and W. AlRcdem (90 miles long).
The swift and muddy current of W. Beht usuaIly"lose4
itself in a swami> before it reaches the main stream. The
imjjetuous Umm Rabi', with a rocky bed and many
rapids, is perhaps as large as the Sebi'i ; but as there are
no important cities in the country through which it flows
its course is not so well known. W. al-Abiad, W. al-Akdur,
and W. Tessaut seem to bo the principal affluents. This-
last is separated by about 10 miles only from the valley
of the Tensfft, the river which flows to the north of the
city of Morocco ; and, by the W. Nefis, the Asif al-Mil'
(Asif is Berber for "river"), the W. Usbi, and other smaller
tributaries, receives the waters of about 180 miles of the
Atlas range. The valley between the Atlas and the Anti-
Atlas is traversed by the W. Siis, whose ever-flowing stream
is sufficient to turn the whole district into a garden. Th&
MAssa or W. al-Ghis (Wholgras of Davidson, Oued Ouel
R'as of Delaporte), though its headwaters drain only one or
two of the lesser valleys at the south-west end of the Anti-
Atlas, is "about 50 yards from bank to bank at the mouth,
with a depth at high water and in the proper channel of
something over a fathom." Farther south is the Assaka
or W. al-AksA, long known to European geographers by the
name of W. Nun ; and finally the famous W. Der'a is
reached, which in length of course exceeds all the rivers of
Morocco, but, except in spring when the snows are melting
in the highlands, remains throughout all its lower reaches
a dry sandy channel, hardly noticed by the traveller in the
surrounding desert. In the upper valleys, on the contrary,
innumerable streams from the south side of the main chain
of the Atlas, the W. Dades from the east, and tbe^Asif
Marghen, W. al-Molah, or Warzazet from the west, flow
through populous and fertile valleys, and uniting to form
the Der'a cut their way southward through a gorge in the
Jebel §ogh^r, which, as the name implies, is a lower range
running parallel to the Atlas proper. For the next 130
miles the noble stream holds south-south-east, drained at
every step by the irrigation canals which turn this region
into a green oasis, till at last its dwindling current bends
westward to the sebkha (salt marsh) of Debiaya. For a
few weeks once a year the thaw-floods fill this shallow but
extensive basin and rush onwards to the Atlantic ; but in
summer it dries up, and, like the bed of the river for some
distance below, is covered with flourishing crops. From
the south of the Atlas still farther east descend a number
of other streams, the W. Ziz (with its tributaries the W.
Todgha and W. Gheris), the W. Ghir, the W. Kenatsa, &c.,
which, after watering the oases of Medghara, TAfflelt
(SijilniAsa), Kenatsa, ic, lose themselves in the sands of
the Sahara.^ Besides the lakes and lagoons of the coast
district already mentioned, there arc several others, such as
the Daya Sidi Ali Mohammed, which Rohlfs passed neat
the summit of the Atlas, but they do not form a feature of
the country. The eastern frontier runs across the great
Western Shatt, and south from that point lies the extensive
Sebkha Tighri.
According to Dr Lcnz, inhisgcologicalmapof West Africa (1882),
the stretch of country in the vicinity of Ceuta and Tetuan is Ju-
r.assic ; modern Tertiary and Eocene rocks cover all the rest of the
gro.Tt northern promontory for some distance south of AVazan, and'
extend in an irregular belt from the ncighbouihood of Fez south-
west to the province of Abda ; between these two areas there lies a
district of Cretaceous formations which extends to the Atlantic, and
skirts the whole African coast from Larash as far south as Capo Blanc
(700 milts south of the Der'a) ; nearly all the rest of the north-
western slope of the country is occupied by alluvium. The west-
ward portion of the Atlas shows a belt of Cretaceous rocks, a broader
Jurassic belt, and one still broader of Red Sandstone, porphyrites
and porplnritic tuffs forming the backbone of the ridge. Fron>
Tarrtdant eastward runs a strip of clay slates, possibly of Carbon-
iferous origin, and from Anti-Atlas in the west and Figig in the
' See Castries on the "Oued Dnii " in liM. de la Sx. (it Glogr.,.
voL.Joa
ceo
PLATE X
!
MOROCCO
833
«r,t Dcvw.ian rncTis stretch for hondredt of milts into the Sahara.
Tne plain around thi city of Morocco has a shoet-like covering of
tufac«ou3 cnj^t rising over hill ajid valley and following all the
undulations of the ground, thu result probably of Iho intense heat
<jf the sun rapidly drawing up water chajgcd with soluble carbonate
of linic from the calcareous strata, and drying it layer by layer on
the surface till an accumulation sciiral feet thick has been produced
(Maw). This crust is extensively burned for lime, and it forms a
natural strong roof for the Diataniorcs or underground cellars which
tlie Jloors excavate in the soft strata beneailu An euormons
deposit of houlJcrs occurs in the lateral valleys and along the
escarpment of the Atlas, and the opinion that these are the pro-
ducts of remote glacial action is supported by the existence of true
moraines in the api>er part of the glens. All along the west coast
there are indications of an elevation of the land in the shape of
raised beaches, at Tangiers 40, at the south of Cape Spartel 50, at
Mogador 60 or 70 feet high ; but a number of other facta seem to
show that at present a process of subsidence is in progress.*
That mineral deposits of great value exist in Morocco there is
Kttlo doubt At Jebel Hadid or the Iron Mountain, the heights
to the north of ilogador, old scoriie are fi>4inQ. In the Bern' Madan
hills near Tetuan are mines, closed, it is said, by the sultan 'Abd
&1-Rahmda; but whether they furnished copper or lead authorities
dilfer. On the road to Eenatsa, Rohlfs saw lead and antimony
vorked by the Beni Sithe. Antimony especially seems to be abun-
dant to the south of the Atlas ; Eohlfs found it in a very pure
state near Tesna, and Dr Alien (whose accdunt was not published
when this article was Avritten) informed tho writer that he saw
spleiidid veins of it north of the Der'a- That gold mines existed
iji Siis was long su.spccted ; Gatell proved it Rock-salt occurs in
the mountains north of Fez, in the valley of the W. MartU, and
jirobably in Jebel Zarhiin. In several places, as in tho route from
Bafli to Morocco, are brino lake^, from which the salt is collected
and exported as far as Central Afnca.
The general as^wct of tho lowlands of Morocco varies «o much
accoi-ding to the season of tho year that, while one stranger finds
it arid and sunburnt and monotonous, another is delighted with the
richness of its ve;;et-vtion and the bright variety of its colours.
Ja some of the Atlas valleys there is a wealth of timber, enormous
eouifers, 10 to 12 feet in girth of stem, oaks, kc.,' but file greater
part of the country has been cleared of every vestige of woodland,
and consctjuently depends for its appearance on herbage, brush-
wood, and the lesser fruit-tre*^j. Cultivation is confined to such
comjurativcly narrow limits that the natural flora has full scoi)e
for Its dcv«lopracnt Cowan, writing more immediately of the
rountry between Morocco and Mogador, speaks of "drifts of as-
phodel, white lilies, blue convolvuli, white broom flowers, thyme
ind lavender, borage, marigold, purple thistles, colossal daisies
and poppies ;" and Captain Trotter tells how for miles the undu-
lating plateau of Kasr Feri'iin was literally covered with »-ild
flowers, whose varied colours, and tho partiality with which ea«h
species eonfmcd itself to certain ground, gave to the landscape a
brilliant and most unique appearance. Dark-blue, yellow, and red
— iris, marigold, aud poppy — occurred in patches an acre in size ;
farther on whole hills and valleys were of a delicate blue tint
from couYolvulus and boi-ago. At times the travelhir's tent is
pitched on a carpet of mignonette, at times on a carpet of purple
bugloss. In tlio country of tho Bcnf H.tsau squills are so abundant
that the fibres of the bulbs are used instead of hair in making tent-
cloth ; and in the north of ICsar al-Kebir the moors are covered for
miles with a beautiful white heathen From such gorgeous cora-
biuatioiis of colour one can well imagine that tho ifooit drew the
inspiration of their chromatic art ; bat the season of floral splen-
dour is bri'.'f, and under tho liot African sun everything soon sinks
into the monotony of straw.
Tho botiny of Jlorocco has been explored by Balansa (1867),
Hooker, Rail, and Maw (1871), Roin and Fritscli (1873), Ibrahim
Amwcriht (a Berber collector, 1873-6), the Rabbi llardochce Abi
Scrur (1872-3) ; and the results have been systematieaMy arranged'
m Cowou's CoMpemiium Fhrx Atlnntica: : o« Flore dcs ilats bar-
i«)vw,,,« (Paris, 1881, kc.).. From tho presence of a largo propor-
tion of nlantsof ceutnil and northern Europe (none of tho northern
plants, however, Ixing of alpine or arctic type) and the absence of
southern types characteristic of the sub-tropical zone Ball concludes
that "the mountain flora of Moroeco is a southern extension of
the European tcniiKTate flora, with little or no admixture of ex-
traneous elements, but so long isolated from tho neighbouring
regions thaj t coiisideraMo number of new specific types have been
developed."' Of the inilividiial plants none are more remarkable
than the ar/lr and the argan. Tho former (Calli/ris quadrivalea.
Thuja nrtUulnOi of Shaw) is a cjiuess-liko tree that grows on the
— 1- -I'iJ!.'- ^'""x^"' »"d Algeria. It furnishes gum sandarach ;
1 >>,.■[. .Miiurlnii In Rull. ,(, rAcnii. h"il. ilr Hcljhpir. voT
«"" rf- h Soc. Cfol. ie France, vol. Iv. ; and especially Ha-
to Hnolicr anfl Ball's .Vororeo.
* Rnlilh Riijr« larelieii, but there hn etronc i
• Compare DniJe, " Florutuclie £rrorsc!li
iSUauavafeu, 1SS2.
1 paper appended
---1 to doubt this.
FlorutiKhe Errorschuns Nord-Afrau's " m Ptlermanifi
1ft— 31
and its beantifurind enduring timber has been identified with the
alerce with which the Cordova cathedral (mosque) was roofed, and
with the citron-wood of the ancient Romans. The argan {Argania
SicUroxyloTi) is confined even in Morocco to a tract of country extend-
ing only about 150 miles along the coast, from the river Tensift
almost to the river Siis, and about 30 miles in breadth ; and it is
found nowhere else in the world. A gnarled trunk and wide-
spreading contorted thorny branches giv(i it a striking appearance.
Large specimens have a height of from 20 to 30 ftct, and a girth of
25 or 26 feet. The fruit, which ripens between May and August, ia
an olire-looking nut, greedily eaten by camels, mules, goats, sheen,
antl homed cattle (bot not by horses) for the fake of the fleshy
pericarp, and crushed by the natives to cxtr.ict tho oil from tho
kernel. Though "its strong and fulsome savour" renders it nauseous
to the European palate, this oil ia largely used in the cookery ol
southern Morocco. The prickly pear forms one of the features
of the landscape from the coast up to the slopes of the mountains.
The cork tree, common in the time of AdcUson, has lost ground
enormously, though it probably forms the staple of the mk'mita
forest, which extends for some 20 miles between the Bii Rakrak
and the Sebu. Though not so widespread as in Algeria or some
disti'Tcts of southern Europe, the palmetto is often locally verj'
abundant Citrons, lemons, limes (sweet and sour), shaddocks,
mulberries, walnuts, and chestnuts are common in many parts.
Tetuan is famous for oranges, Meknes for quinces, Morocco for
pomegi-anates, Fez for figs, Tafilelt and Akka for dates, Siis for
almonds, Dukalla for melons, TaMdast, Ed.intenan, and Rabat for
grapes, and Tariidant for olives (Cowan). The grapo is extensively
cultivated ; the Jews manufacture (Tude but palatable wine^
Sugar, once grown in Sus, to supply the demands of the whole of
Morocco, has disappeared. Bnth hemp and tobacco arc culrivated
under the restrictions of an imperial monopoly, — the former (of
prime quality) being largely used as l^ashisn, the latter, thout^h
never smoked, as snulC Barley is the most usual cereal ; but
excellent crops of wheat, maize, millet, rye, beans, pease, chick-peas,
and canary seed aro also obtained. Potatoes are coming Into
favour in certain districts.
It is still true, as in the time of Addison, that the Moors " seldom,
reap more than will bring the year about," and tho failure of a
single harvest causes inevitable dearth. Captain Colvile calculates
that not more than a hundredth part of the available laud is cnlbi-
vated at all ; and the cultivated portion possessed by each tribe is
divided into three parts, one only of which is sown each year. With
a plough of the most primitive description the Moorish peasant
scarcely scratches the surface of the soil ; and his harrow is a fow
branclKs of trees weighted with heavy stones. The corn is cut close
to the ear with short curved knives, and tho straw left standing.
Undei^ound granaries or matamore^ [inaimura) are constructed,
sometimes capable of holding 2000 quarters ; they preserve their
contents in good condition for many years.
There is abundaut space in the countrj' Cor wild animals, even ofl
the larger kind ; but the absence of woodlaud keeps them in check.
Besides tho lion, which exists only ill very limited numbers, and.
according to local proverbs, with diminished courage, the spotted
leopard, the hyiena, jackal, lynx, fox, and \vild boar are the
most important The auda-d or wild sheep is found in the more
inaccessible parts of the Atlas. Rabbits swarm in the country to
tho north of the Bii Rakrak, and since 1870 they have crossed this,'
whieh used to be their southern limit A kind of ground-squirrel,
the sibsib, occurs in the southern provinces. Monkeys of the sane
species as those of Gibraltar frequent tho neighbourhood of Jebel
Miisa or Apes' Hill. Tho list of the ordinary wild birds includes
blackbirds, goldfinches, linnets, greanfincl'.os, robins, wagtails,
skylarks, and cresitcd larks, as well as turtle-doves, nightingales,
and jays. The house-sparrow is not found ; between Morocco and
Mogador its place is taken by a beautiful bird (Embcriza striola(a\
locally called <a4!6, or "the doctor" (Leaied). The stranger ia
struck by the immense variety and number of hawks, and still more
by the familiar terms on which they build thcir'nests in the. walls
aud rocks along with blue rock-pigoous and starlings. All through
the country the red-legged partridge is the main resource of the
rportsman, though he may also bag other varieties of partridge,
bustards, and ducks and other water-fowl. Along the coasts there
is no lack of gulls, whimbrel, oyster-catchers, &c. Every town has
its colony of storks. LL^rds, chameleons, tortoises, and frogs an
familiar objects ; it is from Morocco that the small tortoises hawked
about tho sheets of London aro usually obtained. The profusion
of insect-lifo is one of the plagues of tho country in the eyes of
tjie European ; and even the Moor, who has got reoonciled to his
mosquitoes and fleas, considers tho locust one of his deadliest
enemies.
Tho camel is the great beast of burden in "Morocco, though asses
and mules are also employed. ,The horse, never reduced to such
base uses, is usually a sturdy little animal, but far below tho
ancient reputation of the Barbary steed. Ronghly broken when
young, hit mouth is soon spoiled by barbarous bits, and his feet
by square shoes. The Imest animals art said to be bred in Shiidme
X.\t — 105
834
MOROCCO
the mnlea are niu
and Abda. In form and sua the mnlea are ninch superior, and
thej •.-.sually fetch two or three timca the price. The horned
oittle are not unlike Aldemeys ; and the sheep, for the iiuproTe-
mont of \riiich nothing i? done, have spiral horns (not untrequontly
four;, rounded foreheads, and long fine wool. Domestic fowb are
kept in groat numbers ; they are of the Spanish tj'pe, small and
prolific. '^
The mackerel fishery off the coast at Casa Blanca and Tangiers
attracts fishers from Spain, Portugal, and other p.irts of Europe.
Oocasionally a small shoal may bo found as far south as Mcador
Soles, turbot, bream, bass, conger eel, and mullet are common°along
the CMst, and a large fish called the aslimsah (rough scaled and
resembling a cod). Lobsters and crayfish swarm in the rocky
places, but the natives have no proper method of catching them
1 he tunny, pilchard, and sardine, and a kind of shad knora aa the
Mogador herring," all prove at times of practical importance.
_ fhe catching of the shMcl or Carbary salmon, a species of shad
)s a groat industry on all the principal rivers of the co.iil, and vast
numbers of the fish, which are often from 5 to 16 pounds in weight
are dried and salted." They ascend from the sta in spring. Bar-
bels and a few other small fish swarm in the streams, but for the
anrfer there is little real sport.'
Of the population of Jlorocco only the vaguest estimate is pos-
sible Behin and Wagner ^ive 6,410,000 — probably too high a
number. Ethnographically it consists of three main elements-
Berbers or Shellnh, Arabs, and Jews— with a large infusion of Negro
blood, and a sprinkling of Negro individuals. A distinction is
sometimes drawn between the country. Arab and the city "Moor "
as he IS called par cxctUrna ; but the difl'erence between them 'is
one not so much of race (though the " Jloor " has probably absorbed
a greater variety of heterogeneous elements) as of method of life,
and the supcificial physical results of the same. The Berbers are
the original occupants of the country (as may V« proved by the
ancient words preserved by classical writers), and they still form
not only the most numerous but the most industrious and civiUzable
section of the people. WhUo the Arab is sHU by preference a dweller
in tents, the Berber for the most part builds himself houses of stone
or clay. On the whole, the Arabs are predominant in the lowlands
and the Berbers in the hilly districts and mountains.
Greatly corrupted, even in the time of Ibn Khaldun, the Arabic
of M/irocco has now, with the complete decav of literature reached
a state of extreme degradation. Of the Schllha dialects very Uttle
13 known, but everything goes to prove theu- general philological
agreement with the better-investigated representative of the Ber-
ber. The Jews are the great commercial class in the community
They are usually said to number about 150,000 to 200,000, but
Kohlfs (Petermann's Milth., 1833) shows reason to suppose that
thev do not exceed 62,800. H.aving come largely from Spain, they
Btlll use among themselves a corrupt Spanish. =
That at one time Morocco was a much mora populous country is
evident froni the description of Leo Afiicanus, though even in his
bme the number of ruined or decaj-ing to^vns was very great
Besides Tangiers, Larash, SaUee, and the other places on the coast
already described, there are only a few large cities in the country.
Fourof theso-FEZ {q.v.), Meknes or Mequinez (y.i..), Wazan, and
\f5?T'"'« ;? th'3 basin of the Sebii. On the Zarhiin range, north
of Meknes^ lies the town of Muley Edris or Zarhiin, which no ghristian
is allowed to enter, though in 1801 Jackson did manage to pay a
burned visit. According to Captain Trotter, who got mthin tliree-
quarters of a mile, it is a place of apparently 1500 to 2000 inhabitants
compact, and with several largo buildings. Wazan (Rohlfs's Wesan) is
par excellence a sacred city, being the seat of a sherif, whose influence
13 even more widely acknowledged than that of the sultan. It was
FT ?i'i^7'"^''i ^^°^ ^ ™"'' ^'""SO ty Muley 'Abd Allih al-Shertf
(06 167.5). _ At present it is one of the cleanest and best-kept places
in the empu-o. Teza (Tiza) is a considerable trading centre on the
route between Fez and the Algerian frontier. Le?, Ali Boy, and
Kohlfs a^ee m descnbing it as a place of great beauty, embowered
in orchards, and the houses give evidence of wealth. Thepopulation,
in Leo 3 tune 20 000, is now 5000, of whom 800 are Jews About
120 milea oast of Tep, and only 10 from the frontier, is Wajda
(Ouchda of the French), clean and noat, in the midst of an oraiir-o
grove. The only other inland toim of importance is Kasr al-Kebu-
(sae Aloaz.^h Kebir), the Oppidum Novum of the Roinans, which,
except on market-days, wears a look of great decay. In all the
country between the basin of the Sebii and the Tonsfft, a distance
of upwards of 200 miles, there is nothing that a European would
consider a town ; and Morocco itself is the only really largo city of
south Morocco. Tirddant, the capital of SiSs, lies between the
Atlaa and the river ; it is a place of from 30,000 to 40,000 inhabit-
ants, has recently been garrisoned and rcfortifiod by tho sulUn
and may bo considered tho frontier city of his empire. High (Ilii-,'
1 A EclontlDc Hut of s
m Ber. Senclc. G*8.^ 1874
;-Vo« a PotUni Storu.
) thirty or foi-ty flfihps from Morocco will bo found
a account of angling oxperlencoa In Payton, Mos^a
•The JTldenoe tor th« rtftonee of > tribe of warUke J«w» In the Ulterior
'■Mnt on the whole to the positive side.
niec, &c.), 100 mile3»aouth-Bouth-ea«t on a stroaia wtich joins tla*
Missa is the chief town of Tazarwalt or the sUte of SidiHiaLani,
an independent principality founded by Sidi Ahmed u Musa ; and
Auguilmin (Gulfmin or Glimin), in like manner, is the d>ief to-«-«
of the state of 'Abd Allah u Salem, or, as it is usually called br
Europeans, Wad Nun. Tagawost (Tagaost of Ibu Khaldiii.i,
about 40 miles inland fiom Ifni, was fom-.eilj iw lalgo city, and
in tho 16th century tho seat of a Spanish factoij nading U' alchil.
Throughout Morocco the nomci claturo of orJu aiy maps gives ■
very misleading idea of tlie numboi of inliabittd site- Most c(
the seeming villages are either markot-placea, completely deserted
except on market-days, or the tombs of saints, with possiblv not i
house in the vicinity, or stations foi caiavaLa, v ith a small ton.
pnnv of soldiers. Tho markets are named after the days of tlw
week, as Siik al-Tbal.'itha, Tuesday maikot ; the kubbas oi "aints'
tombs are distinguished as Sidi (my mastoi) jo aid so ; ai.d th»
stations are marked Nzela, or some such corruption as Iniella.
The prehistoric antiquities of Morocco are of considejable Intel est.
In a cave at Cajjo Spartel M. Tissot found regularly shaped aii-otr-
heads, and in his travels through tho noith of tho country he met
with dolmens, barrows, and cromlechs, just as in Algeria oi Tuni».
The dolmens usually form a trapezium, and the dead body steina to
have been buried \rith the knees drawn up to the chiu. At Mzoiah
(Mazorah), a quaint little vUlago of widely-scattered houses boilt of
rough blocks of yellow soft sandstone, about 8 or 10 miles south-
east from Azili, stands a group of megalithic monuments of ex-
traordinary extent. They have been visited and described by Sii
Arthur de Capell Brooke (1830), Davidson (1833), Farley (1860),
Tissot, Watson, Trotter, ic. Watson's account is the most detailed
Round the base of a mound (16 feet high) of yellow sandstone lie»
a circle of sixty-seven large stones, one of which (at the west sids)
IS more than 20 feet high. In the vicinity are o(?veral other groups,
some of stiU larger blocks. Roman roads seem to ha ve run from Tan '
giere southwards to tho neighbourhood of Jlekned, and from Azilil to
the south of Rabiit ; and Roman sites are in several instances marked
by considerable remains of masonry. At Kasr Fanl'iin (Pharaoh's
castle), on the western slope of J. Zarhiin, are the ruins of VolubiUif.
The enceinte, constructed of large stones and flanked by round towers,
IS 12,000 feet in extent. Four gates are stUl rccogniz-ablc, and a
triumphal arch erected in 216 a.d. in honour of Caracalla and Julia
Domna. The stones of this site have been used for Mekues. Banasa
(Colonia iElia, originally Valentia) is identified with the ruins of Sidi
All Bu Jenun, and Tliamusida with those of Sidi Ali b. Hamed.
At Tchemmish, up the river from Larash, the city of Lixus (Trim
of Strabo) has left splendid specimens of Punic and Roman stone-
work, and the similar remains on the headland of Jliili Bii Selham
probably belong to tho Mudelacha of Polybius. Of early .Moorish
architecture good examples .are comparatively few, and badly pre-
served. Besides those in Fez, Meknes, and Morocco, it is sufficient
to mention the mausoleum of the Beni-Merin (13th to 16th centuries)
at Sheila, which, with the adjoining mosque, is roofless and niined,
but possesses a number of valuable inscriptions (see Athcnanim, 1876).
The present state of Morocco is deplorable. The govenuneut is
an Oriental despotism under an independent quasi-hereditary sultan ;
there are no administrative functionaries with definite responsibility
and regular salary ; the distribution of justice is utteriy arbiti-ary,
and the punishments often barbarous in the extreme ; education,
in the European sense of the word, there is none ; foreign commerco
IS hampered by vexatious prohibitions and restrictions, internal trade
by the almost complete absence of roads and bridges, and by tho
generally lawless state of the country (the very peasant has his gnn
beside him as he ploughs) ; the only substitute for a postal system
IS a class of running couriers; and even the ai-ray (in which tho sultan
does take an interest) is only just beginning to show signs of disci-
plmo and cfTectiveness under the supervision of Kaid M'Clean and
other forei-gu olBcers. The last remnants of tfie once powerful
Moorish fleet are rotting beyondrecognition in the harbour of Larash.
With good government and freedom of trade the country might
soon be restored to a high state of prosperity : its climate, soil,
products, and the qualities of its predominant poi-uLition are full
of promise ; and the evident decrease of hostility towards tho
Christian, which may be observed since the beginning of the cen-
tury, and especially within recent years, gives hope that European
influence, apart from European conquest, may before long remove
from Morocco the reproach of being "the China of the WIst," tho
most backward and barbarous of civilized nations.
^■tjiiory.— Jlorocco corresponds to tho Roman Mauretania Tingi-
tana (.see MADRErANi.\). Connuercd by tiie Vandals (429 a.d )
Mauretania was recovered to the Eastern Empire by BeJisariiia!
The Arabs first peneti'ated into tho country under 'Okba {supra,
p. 567), but the Berbers opposed an obstinate resistance to Islemi
and their conversion and subjection to the caliphate was only com-
pleted iu tho reign of Walid by Mus,i b. Nosair, tho conqueror of
hpain {siqira, p. 673). The dominion of the caliphs was of shocf
duration ; the Abbisids had very little hold of tho Berber countric-
and in the 8th century, while the Aghlabites were practically inde-
pendent at KfllrawiSn, the regions weet of the salt marsh of Sobkhs
MOROCCO
sl-Hedbs were «utonomoiu under » number of in'^igenoiu or foreign
princea. The chief of these principalities were tnat of the Idrisites
»t Fej (rupra, p. 681), the kingdom of Tahart, and that of NikiSr.
In the first years of the 10th centnry the Fitiniite caliphs, at the
bead of the powerful Berber tribe of Ketama, overthrew the AgMa-
bites, thos patting an end for ever to Arab rule in North Africa,
and rapidly extended their empire to the Atlantic. When the Fati-
mites established themselves in Egypt, the Zirid dynasty reigned as
their vassals in the west, and maintained themselves with varying
fortunes till the rise of the great empire of the Almoratides ( j. v. ),
who yielded in turn to the Almohades (q.v.). The latter dynasty
•was eitinguished by the princes of the Beai-Merin, whose chief,
Ya'kilb b. Abd al-Hakk, captured Morocco in 1269 a.d. The sub-
sequent history of Morocco and Fe2 under the Merinids and their
successon presents little interest, being as full of internecine wars,
contested successions, fratricides, general bloodshed, and barbarities
as it is empty of all indications of an advance in civilization. As
regards the relations of the country to European nations, four periods
may be distinguished— (1) a period lasting down to the close of the
Uth century, when the Moorish potentates were still the most pro-
minent representatives of aggressive Mohammedanism ; (2) a period
during which the Portuguese and Spaniards, having expelled their
invaders, made vigorous reprjals and obtained possession of many
towns on the coast of Morocco ; (3) a period in wliich these hations,
disheartened by the disastrous defeat in the Battle of the Threo
Kings (1679), allowed the Moors to recover much of the ground
they had lost, and to become, by their piracies and defiance of inter-
national law, an object if not of terror yet of apprehension and
irntotion ; and (i) a period in which the pr^tige of this after-
glow of greatness has gradually died out.
The following are the more noteworthy events in the Moorish
annals since the beginning of the 15th century.
1416. Ceuta captured by the Portuguese. 1*36. First expedition
against Tangiers by Don Duarte ; capture of Don Fernando, who
died in exile in 1459 (it was proposed to ransom him by cession of
Ceuta, but the pope objected). 1459. Capture of Alcazar Seguir
1471. Captiirj of tangiers. 1610-1540. Bise of the dynasty of the
Shenfs. 1577. Edmond Hogan sent by Queen Elizabeth of England
to Muley Abd al-Melek (see Report in Hakluyt). 1578. Deflat of
King Sebastian (see Leared, Fisit to Court of Morocco, appendix).
1 585. Founding of the Company of Barbary Merchants (earls of War-
mck, ^icester, &c.) in Lonclon ; Elizabeth's second ambassador
Henry Roberts well received. 1610. The Moors from Spain settle
partly at Habat, &c., and prove troublesome. 1649. Muley Zidan
?? . ?v'^'°^ '^i'?.'''^' '• "quoting him to attack Sallee by sea.
About this time Aii Sherif of'Yanbo, near Medina, is recognized as
rnler of TafOelt, and gradually of the rest of the empire except the
city 01 Morocco ; with him commences the dynasty of the Alides •
^L 1««, '^ '°°'- ^'"''^'""^d ^°i Arshid, dispute the succes-
Bion. 1662. Tangiers (Portuguese since 1471) becomes an EnglUh
possession as part of the dowry of Catherine of Braganza. 1664-1672
Keign of Arshid, a warlike, active, and cruel prince, who was the
first to take the title of sulUn. 1672-1727. Reign of Ishmael, who
•n ability and ferocity completely outdid hU brother Arshid, and
rapported his throne by an enormous army of slaves from the
oudin. 1878. Great plague ; ambassadors sent to Louis XIV
^.^ k •"ndof MademoiseUe Blois, the king's natural daughter!
1882. The sultan sends two lions to the king of England. 1684
Sir Cloudesley Shovel defends British interests on the coast ; with-
drairal of the English from Tangiers. 1687. Capture of Larash from
the Spaniards. 1694. Siege of Ceuta. 1725. Thomas Betton. who
had been a slave in Morocco, left £13,000, the half of his fortune
lor the ransom of British captives in that country. 1727-173o'
Disputed succession. 1757-1789. Reign of Mohammed. 1778'
Jfoo o • ''^^' '^''^*' kmiae ; Agadir opened to the Dutch. 1794-
imi. Keign of Sohman ; abolition of Christian slavery in Morocco •
suppression of piracy. 1822-1859. Reign of Abd er Rahman
rupture mth Spain on account of the decapitation of Consul Darmon
■AMI \°""'^"'.S of a Moor. 1844. Defet of forces sent to assist
Abd al-Kader m Algiers ; bombardment of Tangiers and Mogador
by the prince de Jomville ; rout of the Moorish forces in the battle
T»„l- ' * I Pf^fi" ?^ Tangiers. 1845. Naval demonstration at
terri?„rv .^ p" f "^'T^o"' l""*^- ^"rad" to Spain of disputed
l.T,\y »' Ceuta. 1853. Establishment of a customs line and
regular mi itary posts a ong the Algerian frontier, 1856. English
commercial treaty by which no duty shaU exceed 10 per cent of
invalbn' IMrr? ■ 'T.'V\ Reign of MohammeS ; Spanish
ttl MoL „., T? ,\°, ^l'}^ '^*""° C^"^"' O'Donnefi and
tte Moors "ear Tetuan (March). By the treaty of Tetuan Morocco
^nt^C^^^r-T-T ^l^'r *" ^P*'"' to ™"-«»'i" territory at
tZ^ r., « - Y ^^?** ^°' * '=o'n'n"«al establishment, and to
allow the Spanish missionaries to bare a house at Fez like tVit
The t]""^ r fl ''^"^^"•. """'y ■"" bel^robtainrbl' \ pky
the mdemnity. the Spaniards obuined control of the customs for
Lvmrf„r,r ""■ P"f«.I«™itting Europeans to trade in
t^hf / ■°™P"''' 1873. Aocession of Hasan 1880. English
.embassy for improvement of commercial relations; conference at
835
Madrid to Qefine the rights of European representatives in regard
to the protection afforded by them to subjects of the sultan : nnm-
ber of proUgis limited to three. 1882. Expedition to subdue Sid
Hosem of Iligh. 1883. Protest of the English Government against
the slave trade m Morocco.
Lists of wprks iu recard to Morocco wtU be found to Renon, DescHpt. ofonr.'
<i. Ump <U Ataroc, Paris, 1846, forming part of Vcrptor. ttient. d, {AllhZ-
Sji.i'^J? ^- ?«"<";,''« "^T^'i. 18", 1878; and In RUUla Contmp,^n«l',
Madrid 1881. Besides Renou's DticripHm-a. masterly criticism of an provloni
^J^l^J^- ^^ B*""/' Sl=3»); Leo Africanus, J),«rip(. vwS^TSk™^
Tones, Onfen y luceiso <U ios *iri/M . . . de Uarruaos be 1585 M^mrJl
sou Account ofnatBarlarTi, 1671 (Pinkerton'a Coll., it.) ; Chenl4r, RiA. hUt
Sacloo and ffouM, 1820 ; Drummond Hay, irMtern £ar6an/. 18M- John David
t™1' f^i, ^Ik ^if,? ^""■' '" Uormo. Spain, ic, ISsSTRiohM-ds^J
U vols.) ; Boh^s, Be,^ durch itarokko, Bremen, 1868 ; Fritsoh In " Mltthell. i
Vereins fUr Erdk.," Halle 1878; Leared, Morc^ end Ckt M«^ 1875,.™ vii
?vi^l, vt-f"'°£S'' ^f°= De Amlcl-s Uarocco, Milan, IST^s veb- ^phh
£.^fe«^i p f ^^f deservedly tmnslated into EngUsh, French, olniM"
fie. , Tlssot, Btct. tuT to f%r. amparit dt to Jfuaretonij Tinailant. i«n • Oa-
^^^t^^""?-,)}"- ^,"""'"=0', Santiago, 1878; Hooker ind Bku, Afiroo™
and a^ Great Alta,, 1878; Q.tell, I'i^es por Marriucoe. 1879; F^yttr,,M^
W^,„„-^ J."'-,'',""^ 1879; Liana yHodrlgaaez, El imp. de Marluecie, \m:
Watson, AV^t to Waian, 1880 ; Trotter, ifii^on lo tU Court o/Aforocco 18S1 :
Cowan and Johnstone, AfoortiA Lotna Uava, 1882. JKorocoo, isai .
Morocco, or Marocco (Marrdkush), one of the nuasi-
capitals of the sultanate (Fez and Meknes being the other
two), liea in a spacious plain about 15 miles from the
northern underfalls of the Atlas, and 90 mUes east-south-
east of SaflS, at a height variously estimated as 1639
feet (Hooker and BaU), UIO (Beaumier), and 1500
(Leared). Banking during the early centuries of its exist-
ence as one of the greatest and most flourishing cities of
Islam, Morocco has long been in a state of grievous decay
and were it not for the exceptional beauty of its situation'
the luxunant groves and gardens by which it is encom-
passed and interspersed, and the magnificent outlook which
It enjoys towards the mountains, it would be altogether a
very miserable place. The wall, 25 or 30 feet high, and
reheved by square towers at intervals of 360 feet, is so
■dilapidated that foot-passengers, and in places even horse-
men, can find their way in and out through the breaches.
Open spaces of great extent are numerous enough within
the walls, but for the most part they are defaced by
mounds of rubbish and putrid refuse. With the exception
of the tower of the Kutubia Mosque and a certain archway
which was brought in pieees from Spain, there is not, it is
asserted, a single stone building in the city; and even
bricks (though the local manufacture is of exceUent quality)
are sparingly employed. Tdbiya, or pounded clay, is the
almost universal material, and the houses are consequently
seldom raised more than two stories in height. The palace
of the sultan covers an extensive area, and has its parka
and gardens enclosed by walls similar to those of the city
proper, but is architecturally quite insignificant. In the
whole of Morocco the tower of the Kutubia alone is a worthy
memonal of the constructive genius of the early Moors vboth
It and the siniUar towsr of Ha,san at Rabdt are after the type
of the Giralda at Seville, and, if tradition may be trust^
all three were designed by the same architect Jibir. The
mosque to which the tower belongs is a large brick build-
ing erected by 'Abd al-Mumen ; the interior is adorned
with marble pillars, and the whole of the crypt b occupied
by a vast cistern excavated by Mansiir. Other mosques of
some note are those of Ibn Yilsuf, Al-Mansiir, and Al-Mo"izz;
the chapel of Sidi Bel Abbas, in the extreme north of the'
city, possesses property to the value of £200,000, and
serves as a great almshouse and asylum. As in most other
towns throughout Morocco, there is a special Jews' quarter
walled off from the rest. The general population is of a very
mixed and turbulent kind ; crimes of violence are extremely
common, and there are countless varieties of the profes-
sional thief. Almost the only manufacture extensively
prosecuted is that^f Morocco leather, mainly red and
yellow, about 1500 men being employed as tanners and
shoemakers. The city was founded in 1062 by Yiisuf b.
636
M O R — M O K
T^efln. Before it was more than a himdred years old it
is said to have had 700,000 inhabitants, but at present the
total number probably does not exceed 50,000 or 60,000.
Sea Leo Africanua ; Lambert's detailed deecription in Bui. de la
See. de gio^., Paris, 1865; and Dr Lcared's ri/acimeTtto of Lam-
bert. Lambert's plan of Morocco is reproduced with some a^jditions
by Dr Leared ; and another may be found in GatelL (H. A. W.)
MORON, or Mokon be la Feo>jteea, a town of Spain,
in the province of Seville, about 32 miles to the south-
east of that city, occupies an irregular site upon broken
chalk hillocks at a distance of a mile and a half from the
right bank of the Guadaira. It is connected by rail with
Utrera on the Cadiz and Seville Une. On the highest
^elevation, to the eastward are the ruins of the ancient
'eastle, of considerable importance during the Moorish
period, and afterwards used as a palace by the counts of
Ureiia. In 1810-11 it was fortified by the French, but
blown up by them in the following year. The chief public
building of Moron is the large parish church, which dates
from the 16ih century, but presents no noteworthy features.
The fine district between Moron and the Serrania de
Honda is largely occupied by olive plantations, and the
trade in oil and other agricultural produce forms the chief
industry of the town. Moron is also famous throughout
Spain for its chalk (cal de Moron), from which the white-
■wash extensively used in the Peninsula ii derived. The
population of the town was 14,879 in 1878.
)MORONI, GiAiiBATTKTA (c. 1510-1578), an eminent
portrait-painter of the Venetian school, was bom at Albino
near Bergamo about 1510, and became a pupil of Bonvicino
named II Moretto. Beyond the record of his works very-
few particulars regarding him have reached us. Titian,
under whom also Moroni, while still very young, is said
to have studied (but this appears hardly probable), had
st any rate a high opinion of his powers ; h j said that
Moroni made his portraits "living" or "actual" (veri).
And if the magnates of Bergamo came to the great Vene-
tian for their likenesses he advised them to go to their
own countryman. In truthful and animated portraitiu'e
Moroni ranks near Titian himself. His portraits do not
indeed attain to a majestic monumental character; but
they are full of straightforward life and individuality,
witii genuine unforced choice of attitude, and excellent
texture and arrangement of draperies. There is a certain
tendency to a violet tint in the flesh, and Uie drawing
and action of the hands are not first-rate. As leading
eamplos of his portraits may be mentioned — in the Uflizi
Gallery, Florence, the Nobleman pointing to a Flame, in-
scribed "Et quid volo nisi ut ardeat?"; in the National
Gallery, London, the portraits of a Tailor, a member of
the Fenaroli tamily. Canon Ludovico de' Terzi, and others ;
in the Berlin Gallery, his own portrait ; and in Stafford
House, the seated half-figure of the Jesuit Ercole Tasso,
currently termed " Titian's Schoolmaster " — not as indicat-
ing any real connexion between the sitter and Titian,
but only the consummate excellence of the work. Besides
his portraits, Moroni painted, from youth to his latest
days, the ordinary round of sacred compositions ; but in
these he falls'below his master U Moretto, and his design,
which partakes more of the Lombard or Milanese style
than of the Venetian, has at times some of the dryness 'of
the quattrocento. One of the best is the Coronation of the
Virgin in S. Alessandro della Croce, Bergamo; also in the
Cathe<lral of Verona, Sts Peter and Paul, and in the Bn» a
of -Milan, the Assumption of the Virgin. Moroni was
engaged, upon a Last Judgment in the church of Corlago
when he died -on 5th February 1578.
MOPiOSINI, the name of a noble Venetian family.
According to the best authorities, Cappellari and Bar-
baro, there '.vould seem to have been two families of that
name, distinguishing themselves by the variation of tlip'-
shield. The one came from Mantua at the time of Attila's
invasion, and bore or, a fess azure. The other came from
Ulyria in the 7th century ; they bore or, a bend azure.
However that may be, nothing authentic is known of the
Morosini till we find them settled as one family in Venice
during the 8th century. The Morosini belong to the Case
Vecchie, or twenty-four families 6f Venetian nobility who
were descended from the tribunes of the confederate islands
before Venice became united in one centre at Eialto. The
10th century was a period of danger for the family. They
became involved in a blood feud with another noble house,
the Caloprini, who were GhibeUine in poUtics, and relied
upon the emperor Otto for support. The Morosini, how.
ever, proved the stronger, thanks to their popularity ; and
the year 991 saw them victorious through the deposition
of the doge Memo, who had favoured their enemies. The
Morosini engaged in commerce with the East, and in
the 14th century two brothers of the family, Alban and
Marco, founded a house at Aleppo with branches in
Damascus, Beyriit, and elsewhere in Syria. The wealth
and importance of the family may be gathered from the
fact that in 1379 no less than fifty-nine Morosini s-ubscribed
towards the fund for carrying on the war of Chioggia. The
house of Morosini gave four doges to Venice, and numbered
among its honours two royal marriages, two cardinals,
twenty-four procurators of St Mark, besides numerous
generals of the republic. The Morosini continued to
flourish till the opening of the last century, when the
family began "to decline ; it is now represented by one sur-
viving member.
Among the more distinguished members of the house
must be mentioned : — Giovanni, who in 982 founded the
monastic establishment on S. Giorgio Maggiore after the
order of St Benedict; Domenico, doge 1148-1156 — in
the third year of his reign Pola and Istria, which had
rebelled, were reconquered; Marino, doge 1249-1252,
during whose reign the Inquisition, in a modified form and
under the surveillance of Venetian officers, was introduced
into Venice for the firat time. In this same century (1290)
Tommasina Jlorosini, the sister of Albertino il Grande,
married Stephen, prince of Hungary. Their son Andrew
succeeded to the throne, and was directed in his govern-
ment by his uncle Albertino, on whom he conferred the
dukedom of Slavonia and the county of Morlacchia. A
cousin of Tommasina, Costanza, married Ladislaus, king of
Servia. In 1382 Michele Morosini was elected doge.
He had acquired a large fortune and a reputation for
astuteness by bujing Venetian property while the Genoese
were still in Chioggia ; iind much was expected of him in
tha restoration of his country's finance when that war
came to an end. But he died the year of his election.
Andrea Morosini the historian was born in 155S. He
studied at Padua, and on coming of age embarked on
public life. He passed through the various oflices of
state, till in 1618 he was a candidate for the dogeship,
but failed to secure it, and died the same year. On the
death of the oflicial historian Paolo Paruta, in 1598,
Andrea was commissioned by the Council of Ten to con-
tinue his work, and received authority to consult the state
papers down to 1594. He wrote his history in Latin. It
covers from 1521 to 1615, and was first published in
Venice, 1623.
Andrea's other works, of which only tha firsthas been edited, are: —
(1) L'imprase cd csptditioni di Terra Bania e taciiuisto fcJ'o de!V
Impcrio di CostarUinopoli dalla Sermissrma ItcpubUcn di V^tncUa,
T.nice, 1627 j (2) De iU qua Veneta Jiespuilica ad Istrim oras gcssit
adversiis Othonem Federici ImpcrcUorui JiiUim, in the Ccrner-Duodo
collection of Mi^S. ; (3) De forma rcijntbUcw Vindie, ia the National
Library, Pans; (4) RaccoUa dMe Lcgai dr' Cons. X, in th«
Archivio Gcncralc at the Frari, Ysuice ;' (5) D.' rebus geslis ae tuc*
M O R — M O R
837
Frandxi Carmaniola, in the Corner-Dnodo collection. The life of
Andrea han been written by Luigi LoUin, bistop of BeUuno (1623),
ty Niccolo Crasso (1621), and by Antonio Palazzoli (1620).
The most distinguished member of the house of Morosini
■was Francesco, the captain-general of the republic against
the Turks and conqueror of the Morea. He was born in
1318. In 1666 he was in command during an unfortunate
campaign in Candia. In 1687 he conquered Patras, and
80 opened the Morea to the Venetian arms. In the follow-
ing year he was elected doge. After his return to Venice
the republic suffered severely in Candia, and though now
an old man Francesco took the field again in 1693, but
fiied the next year at Nauplia, seventy-six years of age. A
more detailed account of his exploits will be found in the
article Venici
AuOurritiea. — Barbaro, Oenealogie dellc Famiglie Pairizic Venae,
MS., clas. vii. cod. dccccxxvii., in the Marcian Library, Vonico ;
Cappellari, Cainpidoglio Fcnclo, MS., clas. viL cod. ivii., in the
same library ; Komanin, Storia documentata di Venczia ; Freschot,
La Nobilld Venda ; Cicogna, Iscrizione Vcnezianc.
MOEPETH, a municipal and parliamentary borough of
Northumberland, England, is situated in a fine valley on
the Wansbeck, and on the North-Eastem Railway, 50 miles
south of Berwick and 16 north of Newcastle. The Wans-
beck, which is crossed by a stone and t\vo wooden bridges,
winds round the town on the west, south, and east, and
a small rivulet, the Cottingburn, bounds it on tie north.
Morpeth is irregularly built, but possesses a number of
good shops. .The parish church of the Blessed Virgin, a
plain building of the 14th century, is situated on Kirk Hill,
a short distance from the town. Among the other public
buildings are the Edward VI. 's grammar school, reopened
in 1857 after a Chancery suit lasting 150 years ; the town-
hall, erected in 1870 to supersede a building of 1714 by
Vanbmgh ; and the county-hall and former gaol, in the
baronial style, built in 1814. Nothing remains of the old
castle except the gateway. Morpeth had at one time one of
the largest cattle-markets in' England. The industries of
the town include tanning, brewing, malting, iron and brass
founding, and the manufacture of flannels, agricultural
implements, and bricks and tiles. The population of the
municipal borough (231 acrea) in 1871 was 4517, and in
1881 it was 4556. The population of the parliamentary
borough (17,085 acres) in the same years was 30,239 and
33,459.
Morpeth [Morepaih, i.e., the path over the moor) had attained
some size before the Norman Conquest, wken it was granted to
William de Merlay. From the De Merlays it passed tiirougU tU«
Greystocks and Dacres to the Howards, earls of Carlisle. Soon
after the Conquest it obtained the privilege of a market, and
ia 1552 arms were granted to it by Edward VI. It is a borough
by prescription, and waa incorporated by Charles IL By the
Municipal Act of 1835 the government was placed in a mayor and
burgesses, but there is a local board of health distinct from the
corporation, havirfg control over an area slightly larger than that
of the municipal borough. From 1553 the borough sent two
members to parliament, but since 1832 only one member has been
returned, and in 1868 the area of the borough was inctcased.
MORPHEUS is a personification, apparently invented
by Ovid {Metam., xi. 635), of the power that calls up
shapes before the fancy of a dreamer. The name (from
liop<j>^) expresses this function ; Ovid translates it arti/ea
simulaiorque figwrse. Morpheus is naturally represented
as the son of Sleep (Somnus).
MORPHIA. See Opium.
MOEPHOLOGY
THE .term Morphology (/lopi^i), form), introduced by
Goethe to denote the study of the unity of type in
organic form (for which the Linnoean terra Metamorphosis
(q.v.) had formerly been employed), now usually covers
the entire science of' organic form, and will be employed
in this more comprehensive sense in the present article.
§ 1. Historical Outline. — If we disregard such vague
likenesses as those expressed in the popular classifications
of plants by size into herb.% shrubs, and trees, or of
terrestrial animals by habit into beasts and creeping
things, the history of morphology commences with Aris-
totle. Founder of comparative anatomy and ta.Yononiy,
he established eight great divisions (to which are aj)-
pended certain minor groups) — Viviparous Quadrupeds,
Birds, Oviparous Quadrupeds and Apoda, Fishes, Ma-
lakia, Malacostrara, Etitoma, and Oslracodcrmala — dis-
tinguishing the first foiu' groups as Enaima ("with
blood") from the remaining four as Anaima ("blood-
less"). In these two divisions we recognize the Ver-
tebrata and Inver.tebrata of Lamarck, while the eight
groups are identical with the Mammals, Birds, Reptiles,
Fishes, the Ccphalopods, Crustaceans, other Articulates,
and Tcstaceans of recent zoology. Far, too, from com-
mitting the mistake often attributed to him of reckoning
Bats as Birds, or Cetaceans as Fishes, ho discerned the
true affinities of both, and erected the latter into a spe-
cial yekos beside the Viviparous Quadrupeds, far more on
account of their absence of limla than of their aquatic
habit. Not only ia his method inductive, and, as in
, modem systems, his groups patural, i.e., founded on the
aggregate of known char.acters, but he foreshadows such
generalizations as those of the correlation of organs, and
of the progress of development from a general to a special
form, Ioi>g afterwards established by Cuvier and Von
JBaer re.-<pectivelv. In the correspondence he sugggsts
between the scales of Fishes and the feathers of Birds, or
in that hinted at between the fins of Fishes and the limbs
of Quadrupeds, the idea of homology too is nascent ; and
from the compilation of his disciple Nicolaus of Damascus,
who regards leaves as imperfectly-developed fruits, he seemii
almost to have anticipated the idea of the metamorphosis
of plants. In short, we find a knoviledge of structural
facts and a comparative freedom from the errors induced
by physiological resemblance, of which his successors such
as Theophrastus and Pliny, generally mere classifiers by
habit, show little trace, and whi:h the modems have but
slowly regained. Little indeed can be recorded until tlie
13th century, when the reappearance of Aristotle's work*
gave a new impulse to the study of organic nature. Of
the works of this period that of Albertus Magnus is far
the most important; but they ore all no more than re-
vivals of Aristotle, marking the reappearance of scientific
method and the reavrakening of interest in and sympathy
with nature. Meanwhile leech and apothecary, alchemist
and witch, were accumulating coiiiiidcrablo knowledge of
plants, which, after the invention of jirinting, became
collected and extended in the descriptive and well-illus-
trated folios of Gesner and his successors, Fuchs, Lobel,
and others, as well as by the establishment of botanic
gardens and scientific academies, while, as Sachs expresses
it, " in the sharpest contrast to the naive empiricism of the
German fathers of botany came their Italian contemporary
Ca;salpinus, as the thinker of the vegetable world." Both
made systematic efibrts, — the Germans vaguely seclcing for
natural afiinities in mere similarities of habit, the Italian
with no inconsiderable success striving towards an intel-
lectual basis of clas.sification. Monographs on groups of
plants and animal.i frequently appeared, those of Uclon on
Birds and Rondelet on Fishes being among the earliest ; and
in the former of these (1555) we find a comparison of the.
838
MORFHOLOGY
skeletons of Bird and Man in the same posture and as
nearly as possible bone for bone, — an idea which, despite
the contemporaneous renaissance of human anatomy ini-
tiated by Vesolius, disappeared for centuries, unappreciated
save by the surgeon Ambroise V&ii. Palissy, like Leonardo
before him, discerrisd the true nature of fossils ; and such
flashes of morphological insight continued to appear from
time to time during the 17 th century. Thus, Joachim
Jung recogniicd " the distinction between root and stem,
the difference between leaves and foliaceous branches, the
transition from the ordinary leaves to the folia floris," and
Harvey anticipated the generalizations of modem embryo-
logy by his researches on development and his theory of
epigenesis.
The encyolopsdic period of which Qesner is the highest
.representative was continued by AJdrovandi, Jonston,
and others in the 17th century, but, aided powerfully by
the Baconian movement, then profoundly influencing all
scientific minds, it developed rapidly into one of genuinely
systematic aim. At this stage of progress by far the most
important part was taken by John Ray, whose classificatory
labours both among plants and animals were crowned with
marveUous success. He first definitely expelled the fabulous
monsters and prodigies of which the encyclopsedists had
faithfdUy handed on the tradition from medissval times,
and, like his predece^ssor Morison, classifying in a truly
modern spirit by anatomical characters, he succeeded,
particularly among plants, in distinguishing many natural
groups, for which his very terms sometimes survive, e.g.,
Dicotyledons and Monocotyledons, TJmbeiliferae and Legu-
miuosse. The true precursor of Linn:eus, he introduced
the idea of species in natural history, afterwards to become
so rigid and reformed the practice of definition and termino-
logy. Of the many works which followed up Kay's
sj-stematic ar\d monographic labours, though often, Uke
those of Toiu-nefrrt and Eivinus, Reaumur and Klein, of
great importance, none can be even named until we come
to" those of his great successor LirmEEUs, whose extraordinary
grasp of logical method and unparalleled lucidity of thought
and expression enabled him to reform and reorganize the
whole labours of his predecessors into a compact and
definite "systems naturae." The very genius of order,
he established modern taxonomy (see JjIology), not only
by the introduction of the binomial nomenclature and the
renovation of descriptive terminology and method, but
by the subordination of the species — henceforth clearly
defined — under the successive higher categories of genus,
order, and class, so finally reconciling the analytic and
synthetic tendencies of his predecessors. Although the
classification of plants by the number of their essential
organs (which vastly advanced not only the cultivation of
botany but the knowledge of the flora of the globe, and
by which he is popularly remembered) is highly artificial,
it must be remembered that this artificiality is after all
only a question of degree, and that he not only distinctly
recognized its provisional character but collected and ex-
tended those fragments of the natural system with which
Jussieu soon afterwards commenced to build. His classi-
fication of animals, too, was largely natural, and, though
on the whole he unfortunately lent his authority to main-
tain " that disastrous philosophic and scientific aberration "
inherited from the alchemists through the last encyclopsedist
of Gesner's school — the notion of three kingdoms of nature
— he at least at one time discerned the fundamental unity
of animals and vegetables, and united them in opposition to
the non-living world as OrganisaUi. At the same time he
was still far more a scholastic naturalist than a modern in-
vestigator, and his works represent little more than the full
completion of the ancient era, and in the hands of fanatical
followers served often to retard the commencement of the
modem one. So, too, his excesaive systematic and descriptiyt
precision, united as it was with* comparative inattentioo
to other than superficial characters, established a tendency
even yet not extinct, to rest contented with mere method
and nomenclatm'e instead of aiming at complete morpho-
logical knowledge.
While the artificial system was at the zenith of its fame
and usefulness, Bernard de Jussieu was arranging his
garden on the lines afforded by the fragmentary natural
system of Linnaeus. His ideas were elaborated by hia
nephew and successor Antoine de Jussieu, who for tha
first time published diagnoses of the natural orders, so
giving the system its modem character. Its subsec^uent
elaboration and definite establishment are due mainly to
the labours of Pyrame de Candolle and Robert Brown.
The former concentrated his own long life and that of hia
son upon a new " systema naturse," the colossal Prodromia
systcmatis naturcUis (20 vols., 1818-1873), in which 80,000
species were described and arranged. Meanwhile the pene-
trative genius of Erovm enabled him to unravel such struc-
tural complexities as those of Conifers and Cycads, Orchids
and Proteacese, thus demonstrating the possibility of ascer-
taining the systematic position of even the most highly
modified floral types. Both Candolle and Brown were thus
no mere systematists, but genuine morphoiogists of the
modern school. The former, as we shall afterwards see,
established the theory of floral symmetry on grounds of
pure comparative anatomy, and distinguished with greater
success than hitherto between fundamental imity of struc-
tural type and mere superficial similarity of physiological
adaptation. Ite latter (Humboldt's "facile princeps
botanicorum "), using the same ideas with even keener in-
sight, made many memorable anatomical researches, such
as those on the structure of the ovule and the seed, and
indeed by his demonstration of the aflinities of the gym-
nosperms almost anticipated the discoveries of Hofmeister,
who stands pre-eminent among his modem successors on
account of his elucidation of the seoref of phanerogamic
reproduction.
The labours of Bernard and Antoine de Jussieu initiated
too a vast parallel advance in zoology, the joint memoir
on the classification of mammals with which Cuvier and
Geoffrey St-HUaire almost commenced their career receiv-
ing its dominant impulse from the " genera " of Antoine.
Cuvier's works correspond in zoology to those of the
whole period from the Jussieus to Brown, and epitomize
the results of that line of advance. Although in some
respects preceded by Haller and Hunter, who compared,
though mainly with physiological aim, the same parts in
difierent organisms, and much more distinctly by Vicq
d'Azyr, the only real comparative anatomist of the 1 8th cen-
tury, he truly opens the era of detailed anatomical research
united with exact comparison and clear generalization.
The Segne Animal (1817) and the theory of types (verte-
brate, moUuscan, articulate, and radiate) are the results of
this union of analysis and synthesis (although he himself,
exasperated by the aberrations of the Naturphilosophie,
was accustomed to proclaim the importance of detailed
empiricism alone), and mark the reconstitution of taxonomy
on a new basis, henceforth to be no longer a matter of
superficial description and nomenclature but a complete
expression of structural resemblances and diSerences. More
even than Linnaeus he is the founder of a great school,
whose names and labours are imperishable. In Germany,
Bojanus, Meckel, Von Siebold, and the illustrious Johannes
Miiller, with his many living pupils, have carried on the
work ; in France, too, a succession of brilliant anatopiists,
such as De Quatrefages, Milne -Edwards, and Lacaze-
Duthiers, are his intellectual heirs ; and in Englatid he has
been admirably represented by Owen.
MORPHOLOGY
839
The histological moTeijient inaugurated by Bichat will
be subsequently discussed ; the rise of embryology, how-
ever, may be briefly noted, especially since it supplied the
most obvious deficiency of the Cuvierian school Hero the
principal figure is Von Baer, who established independently
the four types of Cuvier on developmental grounds, so for
the first time applying embryology as the touchstone of
anatomical classifications, besides establishing his famous
law of differentiation from a general towards a special form.
It is now necessary to return to Liiinaeus, whose more
speculative -ivritings contain, though encumbered by fan-
tastic hypotheses, the idea of floral metamorphosis (" Prin-
cipium flof um et foliorum idem est," <fec.). About the same
time, and quite independently, C. F. WolflF, the embryo-
logist stated the same theory T,'ith greater clearness, for the
first time distinctly reducing the plant to an axis bearing
appendages — the vegetative leaves — which become meta-
morphosed into bud-scales or floral parts through diminu-
tion of vegetative force. Thirty years later the same view
was again independently developed by Goethe in his now
well-known pamphlet (Vo-such die Metamorphose der
FfMnzen zu erhlaren, Gotha, 1790). In this brilliant essay
the doctrine qf the fundamental unity of floral and foliar
parts is clearly enunciated, and supported by argument?
from anatomy, development, and teratology. All the
organs of a plant are thus modifications of one funda-
mental organ — the leaf — and all plants are in Uke manner
to be viewed as modifications of a common type — the
Urpflan:e. The controversy as to the merits and import-
ance of this essay, and of Goethe's morphological work in
general, can scarcely be entered upon here. That Goethe
discerned and proclaimed, and that more clearly than any
of his predecessors or contemporaries, the fundamental idea
of all morphology — the imity which underlies the multi-
farious varieties of organic form — and that he systematically
applied this idea to the interpretation of the most import-
ant, most complejt, and most varied animal and vegetable
structures, is unquestionable. The difficulties arise when we
aeek to estimate the importance of his works in the chain of
progress, and when we inquire whether, as some historians
hold, his " urpflanze " was a mere ideal archetype, bringing
forth as its fruit the innumerable metaphysical abstractions
of the Naturphilosophie, and leading lus countrymen, to
their fall, into all the extiavagances of that system ; or
whether, as Haeckel maintains, it represented a concrete an-
cestral form, 80 anticipating the view of modern evolutionists.
That to him Schelling was largely indebted for the founda-
tion upon which he erected hia philosophic edifice, as also
that Goethe largely shared the same ideas, is unquestion-
able ; but it must be remembered that he lived and made-
progress for forty years after the publication of this essay,
that he was fanuliar with the whole scientific movement,
and warmly sympathized with the evolutionary views of
Lamarck and Qeoflfroy St-Hilaire ; it is not therefore to
be wondered at that his writings should furnish evidence
in favour of each and every interpretation of them. His
other morphological labours must not be forgotten. Inde-
pendently of Vicq d'Azyr, he discovered the human pre-
maxiUary bone j independently of Oken, he proposed the
vertebral theory of the skull ; and before Savigny, he dis-
cerned that the jaws of insects were the limbs of the head.
In 1813 A. P. de Candolle published his TUorie Ele-
vienlaire de la Botcmique, which he developed into the classic
Organography Vegetale (1827). Although at first unac-
quainted with Goethe's essay, and not clearly discerning the
homology of leaves and floral parts, he established his
theory of symmetry, reducing all flowers to " synmetrical "
groupings of appendages on an axis and accounting for
Mieir various forms by cohesion and adhesion, by arrested or
•Keeidve development. The next great advance was the
investigation by Schimper and Braun of phyllotaxU-^iko
ascending spiral arrangement of foliar and floral organs —
thus further demonstrating their essential unity.
The term morphology was first introduced by Ooelhe
in 1817, in a subsequent essay {Zur Naturvmteruchaft
uberliav.pt, besonders sur Morphologie). It did not come
into use in botany until its popularization by Augtiste do
St-Hilaire in his admirable Morphologie V'egetale (1841),
and in zoology until later, although De Blainville, who
also first employed the term type, had treated the external
forms of animals under "morphologie." Though the Na-
turphilosophie of Schelling and its countless modifications
by his followers, its mystic theories of " polarization " and
the like, its apparatus of assumption and abstraction, hy-
pothesis and metaphor, cannot here be discussed, its un-
doubted services must not be forgotten, since it not only
stimulated innumerable reflective minds to the earnest
study of natural science, but, by its incessant proclamation
of the unity o£ nature and the free use of Platonic arche-
types, gave a most powerful impulse to the study of com-
parative anatomy, and nobly vindicated the claims of philo-
sophic synthesis over those of merely analytic empiricism.
Among its many adherents, some are of more distinctly
theological type, others metaphysical, others mystical or
poetiCj others, again, more e^ecially scientific ; but its
most typical and picturesque figure is Lorenz Oken, who
epitomizes alike the best and the worst features of the
school, and among whose innumerable pseudo- morpholo-
gical dreams there occasionally occurred suggestions of the
greatest fruitfulness, — notably, for instance, the independ-
ent statement of the vertebral theory of the skulL
Although Lamarck shared in this tfiOvetuent^ his great
work (the Philosophie Zoologique, 1809), being setiolo-
gical rather than morphological, scarcely claims discussion
here. By far the most distinguished anatomist of the
transcendental school is Geoffroy St-Hilaire, who being
comparatively free from the extravagances of Oken, and
uniting a depth of morphological insight scarcely inferior
to that of Goethe with greater knowledge of facts and far
wider influence and reputation in the scientific world (which
affected to sneer at the poet as necessarily a mere amateur),
had enormously greater influence on the progress of science
than either. He started from the same studies of anatomi-
cal detail as Cuvier, but, profoundly influenced by Bufibn's
view of unity of plan and by the evolutionary doctrines
of Lamarck, he rapidly diverged into new lines, and again
reached that idea of serial homology of which we have
so frequently noted the independent origin. His greatest
work, the Philosophie Anatomique (1818-1823), contains his
principal doctrines. These are — (1) the theory of unity of
organic composition, ideiitical in spirit with that of Goethe ;
(2) the theory of analogues, according to which the same
parts, differing only in form and in degree of development,
should occur in all animals ; (3) the " principe des con-
nexions," by which similar parts occur everywhere in similar
relative positions ; and (4) the " principe du balancement
des organes," upon which he founded the study of tera-
tology, and according to which the high development of one
organ is allied to diminution of another. The advance in
morphological theory is here obvious ; unfortunately, how-
ever, in eager pursuit of often deceptive homologies, he
wandered into the transcendentalism of the Naturphilo-
sophie, and seems utterly to have failed to appreciate either
the type theory of Cuvier or the discoveries of Von Baer.
He earnestly defended Buffon's and Bonnet's earlier view
of unity of plan in nature ; and the controversy reached
its climax in 1830, when he maintained the unity of
structure in Cephalopods and Vertebrates against Cuvier
before the Academy of Sciences. On the point of fact
he was of coune utterly defeated j the type theory was
840
MORPHOLOGY
thenceforw.ird folly accepted and the Naturphilosophie
received its deathblow, while a " second empiric period "
of exiict aiialomical and embryological research seemed
for ever to replace it. Such was the popular view ; only
a few, like the aged Goethe, whose last literary effort was
a masterly critique of the controversy, discerned that the
very reverse interpretation was the deeper and essential
one, that a veritable " scientific revolution " was in pro-
gress, and that the supremacy of homological and synthetic
over descriptive and analytic studies was thenceforward
assured. The irreconcilablfe feud between the two leaders
really involved a reconciliation for their followers ; theories
of homological anatomy had thenceforward to be strietly
subjected to anatomical and embryological verification,
whUe anatomy and embryology acquired a homological
aim. This union of the solid matter and rigorous method
of Cuvier with the generalizing spirit and philosophic
aims of Geotfroy is well illustrated in the works of Owen ;
and, in short, the so-called Cuvierian school ia in reality
thenceforward also Geoffroyan.
The further evolution of the idea of homology is sketched
below (§ 7), while the extent and rai^idity of the subsequent
progress of the knowledge of all the structural aspects of
plants and animals alike make an historical survey impos-
sible up to the appearance of the Origin of Spea.es (1859) ;
however, no further qimlitative advance was possible, since,
as Sachs has best pointed out, morphology necessai'ily
contains, under the Linnsean dogma of the constancy of
species, the same two inconsistent and irreconcilable lines
of thought which we saw represented by Csesalpinus and
the early German botanists respectively. — on onje side the
want of strictly scientific classification, and on the other
the vaguely-felt existence of a natiu^ relationship. Strict
classification of forms supposed constant excludes in fact any
natwal relationship. The type, theory, the theory of unity
of organic composition, and- the like, are susceptible indeed
of two explanations — they may be regarded as either ex-
pressing a creative plan, or taken as piu-ely Platonic
and archetypal ideas. Both are tenable on theological
and metapliysical grounds respectively, but the fact must
not be disguised that of this unity of type no explanation
in the least degree scientific, i.e., in terms of the pheno-
mena of the natural world, does or can exist. The need-
ful solution was effected by Darwin. The "urpflanze" of
Goethe, the types of Cuvier, and the like, at once became
intelligible as schematic representations of ancestral organ-
isms, which, in various and varying environments, have
undergone difi'erentiatiou into the vast multitude of exist-
ing forms. All the enigmas of structure become resolved ;
"representative" and "aberrant," "progressive" and
"degraded," "synthetic" and "isolated," "persistent"
and " prophetic " types no longer baffle comprehension ;
conformity to type represented by differentiated or rudi-
mentary organs in one organism is no longer contradicted
by their entire disappearance in its near allies, while
systematist and morphologist become related simply as
specialist and generalizer, all through this escape from the
Linn^an dogma of the fixity of species. The phenomena
of individual develojinient receive interpretation in terms
of ancestral history ; and embryology thus becomes divided
into ontogeny and ])hylogeny, the latter, too, coming into
intimate relation with pala>ontology, while classification
seeks henceforth the reconstruction of the genealogical
tree. All these results were clearly developed in the most
important work of the new period, Haeckel's GenerclU
Morphologic (1866), while the valuable contemporaneous
Principles of Biology of Herbert Spencer also gave special
attention to the relation of morphology to physiology.'
* Fo» bibliography «ee Cania, QiaehichU der Zoologii ; S.ichs, Qcs-
§ 2. JterulU. — Though the preceding is but * meagre
outline of the rise and progress of the science, no corre-
sponding sketch of its results can be here attempted. A
description of the refined applications of the doctrine of
floral metamorphosis, an inquiry into the morphology of
the Cryptogams, or an account of such beautiful homo-
logies as those presented by the Arthropods or the Echino-
derms is alike impossible ; . least of all can we consider
the splendid simpliiScation of the supremely complex prob-
lem of vertebrate structure by the elaboration of a new
theory of the skull, and by such luminous discoveries as
those of the segmental organs, or of the origin and homo-
logies of the spinal and cranial nerves. For these organo-
logical conceptions the reader must study such articles. as
those on Amphibia, Birds, Hydkozoa, Mollusca, iSrc,
and such works as those of Huxley, Gegenbaur and
Haeckel, Balfour and Parker, Payer, Eichler, or Asa Gray,
and (provided with the needfal bibliographical equipment
afforded by the various " Jahresberichle " and the kindred
English publications) must indeed also plunge into the
current literature of the science. And there too must be
sought the innumerable attempts at taxonomic synthesis
which such organological progress is constantly originating
(see Akimal Kingdom, Biology, vol. iii. p. 690 sq., and
Vegetable Kingdom). Embryological generalizations,
such as Haeckel's " gastraea theory," Lankester's rival " pla-
nula theory," or the ingenious " ccelome theory " of Hert-
wig, have been recently thoroughly criticized in Balfour's
Embryology. The present article will be confined to a
brief discussion of a few main problems, commencing w-lth
the cell theory aiid the problem of organic individuality
—these being seleoted partly because of their special iUus-
trativeness and intrinsic importance, partly because they
.have somewhat less recently been summarized.
§ 3. Histology — Cell r/icory. —Altiiough the application of tha
simple microscope to the minute structure of plants and animals
had been iu progress since the end of the 17th century, the rise of
modern histology really dates from the Aiuxiomie Geniralc (1801J
of Bichat, which analyses the organism into a series of simple
tissues with definite stmctural characters. This new impulse,
together with the improvement of optical appliances, led to much
further research. "Fibres" and "globules," "laminae" and
"nuclei," were desci-ibed, and even "cells" by Mirbel in 1806,
and in 1835 Johannes Miiller pointed out tlie existence of cells
resembltng those of plants in the vertebrate notochord. The cellu-
lar and nucleated sti^ucture of epidermis and other tissues was soon
demonstrated, while Robert Brovu discovered the nucleus of thft
vegetable cell. In 1833 Schleiden referred all vegetable tissues to
the cellular type, and traced back the plant embryo to a single
nucleated cell, while in 1839 Schwann boldly extended this con-
ception of plant sti'ucture and development to the animal world,
and so fully constituted the "cell theory."
SchA^-ann's cells were essentially nucleated vesicles with fluid
contents which originated in an intracellular substance ; but thia
view was soon abandoned. Dujai-diu had discovered that the bodies
of Foraminifera were composed of a viscous gianular contractile
sarcode, and Ton Mohl described independently iu similar terms
tlie contents of the vegetable cell as protoplasm. This was identi-
fied by Max Schultzo as Dujardin's sarcode, the newer name sur-
viving ; and this living matter, and not the membi-anc, he showed
to be the essential constituent of the cell, since which his amended
definition of the cell as a unit-mass of nucleated protoplasm has
been generally accepted. Prevost and Dumas had noticed th«
segmentation of the ovum into misses as early as 1824, and these
were naturally identified as cells innnediately after the publication
of Schwann's work. In 1846 Kdllikcr showed that all tissues aiisa
from these segmentation masses, and that the multiplication of
animal and vegetable cells takes place by a continuation of th«
same piocess, — that of tiansverse division already obser\'ed in th'«
Protozoa.
These points gained, the attention of liistologists was withdrawn
for a considerable time from the scrutiny of the minute structur*
of the cell itself to be concentrated on tlie modes of origin of these
unit-masses, and their subsequent ditTerentiatiou and aggregation
into tissues and organs. The minute structure and histogenesis of
thichu d. Botanik ; Cuvier, HUt. d. Set. ; Is. G. St-Hilaire, UiiL Kat:
Gen.: Masters •in Mld.-CluT. Rev., 1658, So.; also articles GoETHK,
LISM.KDS, OUSS, &C
M O R P H O L O G Y
841
plants, as well aa of at least the higher animals, hare been stndied
with much and over-increasing accuracy of detail. (See Ana-
tomy, Histology, Embryoloot.) Both vegetable and animal
tissues hare been simply classified both according to their adult
fonns and according to the embryonic layers from which they
respectively arise. This eorutiny of plant and animal structure
over and above the special generalizations of the botanist and the
zoologist has afforded much result to general histology. The
improvement of technical methods' has of late years largely aided
the progress of discoYcry. A return from the study ol the cell-
Xgate to that of the cell has commenced, and the qneetipn of
tructure may be said to be again paramount in histology. The
process of transverse division has of late been much elucidated,
and, although its complex details cannot her« be entered npoo,
the result has been to establish a minute and thorough correspond-
ence in cases so widely dissimilar as pollen-grains from a flower-bud,
the epidermis of a tadpole, or the cells of a tumour — a result which
©bvioualy enhances tne morphological completeness of the cell
theory. Minor modes of cell-multiplication also are not without
their morphological interest. Gemmation, familiar in the yeast
plant, occurs in other low and simple organisms, and may probably
06 identified with the formation of polar vesicles in ova as a modi-
fication of transverse division. Schleiden had supposed all new
cells to originate within pre-existing cells, and this process, known
as free -cell-formation, may really be observed in various plant
and animal tissues. The protoplasm groups itself round new nuclei,
the new cells being in fact formed much as Schwann bad in his
turn 8upp(wed ; but these nuclei have repeatedly been shown to
arise from segmentation of the original nucleus, and thus this pro*
cess too seems a mere modification of the general one of transverse
division. Conjugation, too — that coalescence of two similar cells
which may be observed in .many Algae, Fungi, and Protozoa — is to
be considered as the undifferentiated form of that fertilization which
occurs in higher animals and plants, the two apparently similar
masses having become respectively differentiated into ovum and
spermatozoon, or into eg^-cell and antherozoid. An indefinite
number of amoeboid cells, sometimes flow together into a single
mass, — a phenomenon regatded by some as multiple-conjugation,
or perhaps more probably as an almost mechanical coalescence of
exhausted cells, from which conjugation proper and finally fertili-
zation may indeed have originated. The amoeboid cells of higher
animals similarly unite when drawn, and this formation of plas'
modia, as these are termed, seems to be a deep-seated property of
the amoeboid celL Similarly, too, the process of rejuvenescence
which occurs in many of the lowest plants and animals, such as
Protococcus and Amoeba, where the protoplasm passes from a rest-
ing and encysted to a naked and mobile stage, has many analogues
not only among the Protista but even in the tissues of higher
animals, while the phases which the lowest organisms more or less
fxhibit— the encysted, the ciliated, the amoeboid, and the plasmo-
dtal — may be regarded as the fundamental forms of a "life-cycle,"
fully represented indeed only in euch extremely low organisms as
Protomyxa and Myxomycetes, yet nowhere completely suppressed.
The very highest plants and animals may thus be considered as
aggregates, of more or less differentiated and variously arranged
encysted, ajnceboid, and ciliated cells, while their development
and subsequent changes, their variations normal and pathological,
in reality exhibit phases more or less distinct of the ancestral life-
cycle.
The examination of the precise modes of cell-division, particularly
in the hands of botanists (see Biology, and summary in Sachj^'s
Vorksungen Ubcr PJlanzcn Physiologic, 1883), are also constantly
throwing the most interesting light upon the structure of the adult
organism. Thus then, in our own day as in those of Bichat or
Schwann, the labours of the hiatologist, when inspired by higher
aims than that of the mere multiplication of descriptive detail, are
of supreme morphological importance, and result in the demonstra-
tion of a unity of organic structure deeper even than any which we
owe to Linnaeus or Cuvier, Goethe or Geofiroy^
§ 4. Individuality. —ViohdhXy no subject in the whole range of
biology has been more extensively discussed than that of the nature
of organic inJi\nduality. The history of the controversy is of
interest, since besides leading up to solid results it sen-es, perhaps
better than any other case, to iilustrate the slow emergence of the
natural sciences from the influence of scholastic thought Storting
from the obvious unity and indivisiblenessof Man and other higher
animals, and adopting some definition such as that of Mirbel
(exceptionally unmetaphysical, however), "Tout 6tre organise,
complet dans ses parties, distinct et separe des autres etres, est un
individu," it was attempted times -without number to discover the
same conception elsewhere in nature, or rather to impose it upon
all other beings, plants and animals alike. The results of different I
inquirers were of course utterly discrepant.- It seemed easy and
natural to identify a tree or herb corresponding to the individual
animal, yet difficulties at once arose. Many apparently distinct
plants may arise from a commou root, or a single plant may be
decomposed into branches, twigs, shoota, buds, or ev^n leaves, &U
often capable of separate existence. These, again, are d«compO0-
able into tissues and cells; the cells into nucleus, &c., and ultimately
into protoplasmic molecules, these finally into atoms, — the inquiry
thus passing outside organic nature altogether and meeting the olil
dispute as to the ultimata divisibility of matter. In ^ort, as
Haeckel remarks, scarcely any part of the plant can be named
which has not been taken by some one for the individual. It is
necessary, therefore, briefly to notice some of the principal works
on the subject, and these may conveniently be taken in descending
order.
While Cassim practically agreed with Mirbel in attempting to
regard separate plants as individuals, the widest interpretation of
the individual is that of Gallesio (1816), who proposea to regard
as an individual the entire product of a single seed, alike whether
this developed into a uni-ajoal plant extended continuously like a
Banyan, or multiplied aseiually by natural or artificial means like
the Weeping-willow or the Canadian Pondweed, of each of which,
on this view, there is only a sin^e individual in Britain, happily
discontinuous.
At once the oldest and most frequently maintained view is that
which regards the bud or shoot consisting of a single axia with
appendages as the plant-individual, of which the tree represents a
colony, like a branched hydroid Polyp. This conception, often
attributed to Aristotle, but apparently without foundation, appears
distinctly in the writings of Hippocrates and Theophrastus, — the
latter saying, "The bud grows on the tree like a plant in the ground."
The aphorism of Linnaus, "Gemmae totidem herba," is wellknown ;
and in this view C. F. Wolff and Humboldt concurred, while
Erasmus Darwin supported it by an appeal to the facts of anatomy
and development. Tne most influential advocate of the bud theory
during th^ first half of the present century was, however, Du Petit-
Thouars, who, although starting much as usual with a "principe
unique d'existence, " supported his theory on extensive though
largely incorrect observations on stem structure and growth. Fw:
him the tree is a colony ofphyi^nSf each being a bud with its axillant
leaf and fraction of the stem and root. Passing ovei numerous
minor authors, we come to the central work of Alex. Braun (1853),
in which, as Sachs has clearly pointed out, the illegitimate com-
bination of Naturphilosophie with inductive morphology reaches
its extreme. He reviews, however, all preceding theories, admits
the difficulty of fixing upon any as final, since the plant, physio-
logically considered, is rather a divi^uum than an individmnn , and
proposes as a compromise, or indeed as a partial cutting of the
knot, the adoption of the shoot as the morphological individual,
comparable to an animal, esi>ocialIy because, unlike the cell, leaf,
&c., it includes all the representative characters of the species.
Darv.in and Spencer on the whole also accept the bud or shoot as
at any rate the most definite individual.
The theory of metamorphosis naturally led Goethe, Oken, and
others to regard the leaf as the individual, while Johannes Mullei;
Steenstrup, and others adopted the same view on various physio-
logical grounds. Gaudichaud elaborated a theory intermediate
between this view and that of Du Petit-Thouars, according to which
the plant was built up of individuals, each consisting of a leaf ^vith
its subjacent intemode of stem, which was regarded as the leaf-base,
and this was supported by Edwai*d Forbes and others, while the
nominally converse view — that of the leaf as a mere outward ex-
pansion of the stem-segment — was proposed by Hochstetter,
Though sundry attempts at identifying various tissues, such aa
the fibro-vascular bundles, as the constituent individuals may b^
passed over, those associated with the ceU theory are of great
importance. Schwann decided in favour of the cell and Regarded
the plant as a cell -community, in which the separate elements were
like the bees of a swarm, — a view virtually concurred in in all
essential respects by Schleiden, Virchow, and other founders of the
cell theory. Yet, although the structure and functions of the plant
are ultimately and exclusively cellular, it is impossible to ignore
the fact that, save in the very lowest organisms, these are subordi-
nated and differentiated into larger aggregates, and form virtually
but the bricks of a building, and hence the later theories outlined
above. Of attempts to find the individual iu the nucleus or the
protoplasm granules it is of course unnecessary to speak further.
So far the theories of absolute individuality. The conception of
relative individuality is well traced by Fisch upwards from the
more or less vague suggestions in the writings of Goethe, Roeper,
and the elder De Candolle to its clear expression in Alphonse de
Candolle and Schleiden, both of whom take the cell, the shoot, and
the multi-axial plant as forming three successive and subordinated
categories. Nageli too recognized not only the necessity of establish-
ing such a series (cell, organ, bud, lealy axis, multi-axial plant)
but the distinction between morphological and physiological in-
dividualities afterwards enunciated by Haeckel,
Passing over the difficulties which arise even among the Protozoa
(see ForahinifeKa), we find that a similar controversy (fully
chronicled in Haeckel's Kalkschw&mnu) has raged over the in-
dividually of Sponges. While the older obsarvers were content to
regard each sponge-maas as an individual, a view in which Liebe*kuhn
XVI. — io6
842
MORPHOLOGY
and other jnonographere substantially concurred, tte application of
the microscoiw led to the view suggested by James Clark, and still
stoutly supported by Saville Kent, that the Spongo is a city of
amceboid or infusorian individuals. Carter looked upon the separate
ampullaceous sacs as the true individuals, while Schmidt, defining
tlic individual by the possession of a single exhalent aperture, dis-
tin-niishes Sponges into solitary and social. Later, however, he
terms them 2oa impersoTialia.
For the higher animals the problem, though perhaps really even
Eioro difficult, is less prominent. As Haeckel points out, the earlier
discussions and even the comparatively late essay of Johannes
Mullcr take an almost purely psychological or at least a physiological
point of view ; and the morphological aspect of the inquiry only
came forward when the study of much lower forms, such as Cestoid
"VVonns (see Plaia^helminthes) or Siphonophorcs (see Htdrozoa),
had raised the difiiculties with which botanists had so long been
familiar. "With the rapid progress of embryology, too, arose new
problems; and in 1S42 Steenstrup introduced the conception of an
' ' alternation of generations" as a mode of origin of distinct individuals
by two methods, for him fundamentally similar, the sexual from im-
pregnated females and the asexual from unimpregnated "nurses," —
a view adopted by Edward Forbes and many other naturalists, but
keenly criticized by Carpenter and Huxley. In Lcuckart's remark-
able essay on polymorphism (1853) the Siphonophora were analysed
into colonies, and their varied organs shovrn to be morphologically
equivalent, while the alternate generations of Steenstrup were
reduced to a case of polymorphism in development. Leuckart
further partly distinguished individuals of different orders, as well
as between morphological and physiological individuals.
In 1852 Huxley proposed the view which he still substanbially
maintains (see Biology). Starting from such an undoubted homo-
logy as that of the egg-producing prpcess of Hydra with a free-
swimming Medusoid, he points out that the title of individual, if
applied to the latter, must logically be due to the former also, and
avoids this confusion between organ and individual by defining the
individual animal, as Gallesio had done the plant, as the entire
Sroduct of an impregnated ovum, — the swarm of Aphides or free
[edusae which ia this way might belong to a single individual being
tenired Zooids.
In Carus's System of Animal Morphology (1853) another theory
was propounded, but the problem then seems to have fallen into
abeyance until 1865, when it'forrned the subject of a prolonged and
fruitful discussion in the Principles of Biology. Adopting the cell
(defined as an aggregate of the lowest order, itself formed of physio-
logical units) as the morphological unit, Spencer points out that
tliese may either exist independently, or gradually exhibit unions
into aggregates of the second order, like the lower Algie, of which
the individuality may bo more or less pronounced. The union of
such secondary aggregates or compound units into individuals of a
yet higher order is then traced through such intermediate forms as
are represented by the higher seaweeds or the Liverworts, from the
thallus of which the axes and appendages of Monocotyledons and
Dicotyledons are ingeniously derived. The shoot of a flowering-
plant is thus an ag^egate of the third order ; it branches into an
aggregate of the lourth or higher order, and finally as a tree
"acquires a degree of composition too complex to be any longer
defined." Proceeding to animals, the same method is applied.
The Protozoa are aggregates of the first order. These, like plants,
exhibit transitions, of which Radiolarians, Foraminifera, and
Sponges are taken as examples, to such definite compound wholes
as Hydra ; and such secondary aggregates multiply by gemmation
into permanent aggregates of the third order^ which may exhibit
ail degrees of integration up to that of the Siphonophora, where
the individualities of the Polyps are almost lost in that of the
aggregate form. The whole series of articulated animals are next
interpreted as more or less integrated aggregates of the third order,
of which the lower Annelids are the less developed forms, the
Arthropods the more highly integrated and indi^-idualizedt Molluscs
and Vertebrates are regarded as aggregates of the second order.
In 1866 appeared the latest morphological filassic, the GenerUlc
Mcrpliologie of Haeckd. Here pure morphology is distinguished
into two sub-sciences, — the first purely structural, Udology, which
regards the organism as composed of organic individuals of difierent
orders ; the second essentially stereometric, promorpkology. To
tectology, defined as the science of organic individuality, a large
section of the work is devoted. Dismissing the theory of absolute
individuality as a metaphysical figment, and starting from the
view of Schleiden, De CandoUe, and Nageli of several successive
categories of relative individuals, he distinguishes more clearly than
heretofore the physiological individual (or Hon), characterized by
definitcness and independence of function, from the morphological
individual (or morphon), characterized similarly by definiteness of
form ; of the latter he establishes six categories, as follows : —
1. Plastitks (cvtodes and colls), or elementary organisms.
2. Organs (cell-stocks or cell-fusions), simple or nomoplaatic or-
pans (tissues), or hetoroplaatic organs. Organ -systems, organ-
apparatuses.
3. Antivxercs (opposite or eymmctrical or homotypic parts), e.g.,
rays of radiate animals, *' halves of bilaterally sytnmetxicBl
animals."
4. Mctameres (successive or homodynamous jiarts), e.^., stem-
segments of Phanerogams, segments or zoonites of Ajinelidt
or Vertebrates.
5. Tcrsonm, shoots or buds of plants, polyps of Ccelenterates,
&c., " individuals " in the narrowest sense among the higher
animals.
6. Conns (stocks or colonies), e.g.t trees, chains of Salpse, polyp*
stocks, &c
In his subsequent monograph on calcareous Sponges, and in &
final paper, he somewhat modifies these categories by substituting
one category of extreme comprehensiveness, that of the idorgan^ in
place of the three separate orders of organs, antimeres, and meta-
meres. The idorgan (of course clearly distinguished from the
physiological organ or biorgan) is finally defined as a morphological
unit consisting of two or more plastids, which does not possess the
positive character of the person or stock. These are distinguished
into hornoplasts or homo-organs and alloplasis or alloe-organs, the
former 'including, as subdivisions, plastid -aggregates and plastid-
fusions, the latter idomeres, antimeres, and metameres. The former
definition of the term antimere, as denoting at once each separate
ray of a radiate, or the right and left halves of a bilaterally sym-
metrical animal, is corrected by terming each ray a paraw^e, and its
symmetrical halves the antimeres. Thus an ordinary Medusoid haa
four parameres and eight antimeres, a Star-fish five and ten. The con-
ception of the persona is largely modiiied, not only by withdrawing
the comparison of the animal with the vegetable shoot and by omit-
ting the antimere and metamcre as necessary constituents, but by
taking the central embryonic form of all the Metazoa — the gastrula
(fig. I) and its assumed ancestral representative, the gastra
the simplest and oldest form of per-
sona. The different morphological
stages to which it may attain are clas-
sified into three series : (1) Monax-
oniaP inarticulate persons, i,c., uni-
axial and unsegmented without anti-
meres or metameres, as in Sponges, or
lowest Hydroids ; (2) Stauraxonial ^
inarticulate persons with antimeres,
but without metameres, e.g.. Coral,
Medusa, Turbellarian, Trematode, Bry-
ozoon ; (3) Stauraxonial articulate per-
sons with antimeres and metameres,
c.j;., Annelids, Arthropods, Vertebrates.
The colonies of Protozoa are mere idor- Fio. 1.— Gastrula in optical sec-
gana. Ti-ue corms composed of united ^°a"'S°S?J"Si,'r;(?rS
personae, occur only among Sponges, pore and arch-enteron), as alao
Hydroids, Siphonophorcs, Corals, Bry- outeranduinerlayers.ectoderm
ozoa, Tunicates, and Echinoderms, of audendoderm. (After HaeckeL)
which the apparent parameres are regarded as highly centralized per-
sonie of a radially-budded worm colony; and these can be classified
according to the morphological rank of theii* constituent personec
They usually arise by gemmation from a single persona, yet in Sponges
and Corals occasionally by fusion of several originally distinct
persons or corms. The theory of successive subordinate orders of
individuality being thus not only derived from historical criticisn
of previous theories but brought into conformity with the actual
facts of development and descent, — various gi-oups of organisms
being referred to their several categories, — the remaining problem
of tectoloffy, that of the relation of the morphological to the physio-
logical individuality, is finally discussed. Of the latter, three cate-
gories are proposed :---(l) the "actual bion or complete physiological
individual," this being the completely developed organic form which
has reached the highest grade of morphological individuality proper
to it as a representative of, e.g., its species ; (2) the "virtual bion
or potential physiological individual," including any incompletely
fleveloped form of the former from the ovum upwards ; and (3)
the "partial bion or apparent physiological individual," such frag-
ments of the actual or virtual bion as may possess temporary inde-
pendence without reproducing the species— this latter catogoiy
having, however, inferior importance.*
Haeckel's theory, indeed in its earlier form, has been adopted by
Gegenbaur and other morphologists, also in its later form by Jiiger,
who, however, rejects the category of idorgan on the ground of the
general morphological principle that every natural body which
carries on any chemical changes with its environment Decomes
dificrentiated into more or less concentric layers ; but the subject,
especially as far as animals are concerned, is again recently dis-
cussed in a largo work by Perrier. Starting from the cell or plastid,
he terms a permanent colony a miride, and these may remain
isolated like Sagitta or Rotifer, or may multiply by gemmation to
1 Far explanation of these t-cnns see § 5, Promorpholo"^, u M4.
* For criticism of this theory on tlie ground of its maki ic ^iiyBioloffical de-
pend OD luorpholoeical individuality, see Fiacli, Aufa&Jduno tifu* KtUxU d*r
vtTKhudtTun AnsimUu iiber da< pJ1aruIicA« /ndivldvum, p. U.
MORPHOLOGY
843
form higher aggregates which he terms zoida. Such zoides may be
irregular, radiate, or linear aggregates, of which the two former
classes especially are ternxed dijjus. The organ — Haeckel's idorgan — .
is excluded, since tissues and organs result from division of labour
in the anatomical elements of the merides, and so have only a
■econdary individuality, "carefully to be distinguished from the
individuality of those parts whose direct grouping has formed the
organism, and which live still, or have Uved, isolated from one
another." Perrier further points out that undifferentiated colonies
are sessile, as Sponges and Corals, while a free state of existence is
associated with the concentration and integration of the colony into
tn individual of a higher .order.
So far the various theories of tho subject ; detailed criticism is
impossible, but some synthesis and reconciliation must be attempted.
Starting from the cell as the •morphological unit, wo find these
forming homogeneous aggregates in some Protozoa and in the early
development of the ovum. But integration into a whole, not,
merely aggregation into a mass, is essential to the idea of individu-
ality; the earliest secondary unit, therefore, is the gastrula or
m^ride. This stage is permanently represented by an unbranched
Hydra or Sponge or by a Planarian. These secondary units may,
however, form aggregates either irregular as in most Sponges, in-
definitely branched as in the Hydroids and Actinozoa, or linear as in
such Planarians as Catenula. Such aggregations, colonies, or demes,
not being aggregated, do not fully reach individuality of the third
order. This is attained, however, for the branched series by such
forms as Siphonophores among Hydrozoa, or Henilla or Pennatula
among Actinozoa ; for linear aggregates again by the higher Worms,
and still more fully by Arthropods and Vertebrates. Aggregates
of a yet higher order may occur, though rarely. A longitudinally
dividing Nais or laterally branched Syllis are obviously aggregates
of these tertiary units, which, on Haeckel's view, become integrated
in the Echinoderm, which would thus reach a complete indivi-
duality of the fourth order. A chain of Salpse or a colony of Pyro-
■oma exhibits an approximation to the same rank, which is more
nearly obtained by a radiate group of Botryllus around their central
cloaca, while the entire colony of such an Ascidian would represent
tho individual of the fifth order in its incipient and unintegrated
state, — these and the preceding intermediate forms being, of course,
readily intelligible, and indeed, as Spencer has shown, inevitable
on the theory of evolution.
The exclusion of tissues and organs from rank in this series is
thus seen to necessarily follow. Ectoderm and endoderm cannot
exist alone ; they and the organs into which they differentiate
arise merely, as Jager expresses it, from that concentric lamination,
or, with PeiTier, from that polymorphism of the members of the
colony, which is associated with organic and social existence. Tho
idea of the antimere is omitted, as being essentially a promorpho-
logical conception {for a Medusoid or a Star-fish, though of widely
distinct order of individnality, are equally so divisible) ; that of
Oxe metamere is convenient to denote the secondary units of a
linear tertiary individual ; the term persona, however, seems un-
likely to survive, not only on account of its inseparable psycho-
logii^ connotations, but because it has been somewhat vaguely
applied alike to aggregates of the second and third order ; and the
term colony, corm, or deme may indifferently be applied to those
•Sgregates of primary, secondary, tertiary, or quaternary order which
are not, however, integrated into a whole, and do not reach the
fuU individuality of the next higher order. The term zooid is also
objectionable as involving the idea of individualized ofgkns, a view
natural while the medtisoid gonophores of a Hydrozoon were looked
at as evolved of its homologue in Hydra, whereas tlio latter is
really a degenerate form of the former. Passing to the vegetable
■world, here as before the cell is the unit of the first order, while
aggregates representing almost every stage in the insensible evolu-
tion of a secondary unit are far more abundant than among animals.
Complete unity of the second order can hardly be allowed to the
thallus, which Spencer proposes to compound and integrate into
tertiary aggro^tes— the higher plants ; as in animals th^ embryo-
logical method is preferable, both as avoiding gratuitous hypothesis
and as leading to direct results. Such a unit is clearly presented
by the embryo of higher plants in which tho cell-aggregat 3 is at
once differentiated into parts and integrated into a whole. Such
an embryo possesses axis and appendages as when fuUy developed
(fig. 2). The latter, however, being as organs mere lateral expan-
sions of the concentiic layers into which the plant embryo, like the
animal, is differentiated, and so neither stages of evolution nor
capable of separate existence, are not entitled to individual rank.
The embryo, the bud, shoot, or uniaxial plant, all thus belong to
the second order of individuality, like the Hydroid they resemble.
Ijke the lower C<elenterates, too, aggregates of such axes are
fornied by branching out from their low degree of intcgi-ation.
Such colonies can hardly bo termed individuals of the third, much
less of higher order, at least without somewhat abandoning that
unity of treatment of plants and animals witliout which philo.ophi-
ea biology disappears. Individuality of tlie second order is most
lully reached by-the.flQwer,—tht~jaosU^sti^differentinted and
integrated form of axes and appendages. Such a simple inflores-
cence as a raceme or umbel approximates to unity of the third order,
towhich acomposite flower-head must
be admitted to have attained, while a
compound inflorescence is on the way
to a yet higher stage.
If, as seems probable, a nomencla-
ture be indispensable for clear ex-
pression, it may be simply arranged
in conformity with this view. Start-
ing from the unit of the first order,'
the plastid or monad, and terming v
any undifferentiated aggregate a cJcm«,
we have a moiuid-dcme integrating .,
into a secondary unit or dyad, this ^',°w o^'T^", °' Dicotj-ledon
rising through dyad^enus into a t^' ^'^'i^.Z^l'^^'^'Sl
triad, this forming triad-deincs, and the three coDcentric embrvonic
these when differentiated becoming layers.
UiTods, the BotryUus-colony with which the evolution of compound
individuality terminates being a tetrad-denu. The separate living
form, whether monad, dyad, triad, or tetrad, requires also some dis-
tinguishing name,forwhich persona will probably ultimately be found
most appropriate, since such usage is most in harmony with its inevi-
table physiological and psychological connotations, while the genea-
logical indiridualof Gallesio and Huxley,common also to all the cate-
gories, may be designated with Haeckel the ovum-product or ovum-
cycle, the complete series of forms needed to represent the species
being the spccies-cycU (though this coincides with the former save
in cases where the sexes are separate, or polymorphism occurs).
For such a peculiar case as Diplozoon paradoxum, where two
separate forms of the same species coalesce, and still more for such
heterogeneous indiriduality as that of a Lichen, where a composite
unit arises from the union of two altogether distinct forms — Fungus
and Alga, — yet additional categories and terms are required.'
§ 5. Pr<muirpliology.—3\is,t as the physiologist constantly seeks
to interpret the phenomena of function in terms of mechanical,
physical, and chemical laws, so tho morphologist is tempted to
inquire whether organic as well as mineral forms are not alike
reducible to simple mathematical law. And just as the crystallo-
grapher constructs an ideally perfect mathematical form from an
imperfect or fragmentary crystal, so the morphologist has frequently
attempted to reduce the complex-curved surfaces of organic beings
to definite mathematical expression.^ Canon Moseley (i'Art. Trans.,
1838) succeeded in showing, by a combination of measurement and
mathematical analysis, that the curved surface of any turbinated
or discoid shell might be considered as generated by the revolution,
about the axis of the shell, of a curve, which continually varied its
dimensions according to the law of the logarithmic spiraL For
Goodsir this logarithmic spiral, now carved on his tomb, seemed
a fundamental expression of organic curvature and the dawn of a
new epoch in natural science — that of the mathematical investiga-
tion of organic form — and his own elaborate measurements of the
body, its organs, and even its component cells seemed to yield,
now the triangle, and again the tetrahedron, as the fimdamental
form. But such supposed results, savouring more of the Natur-
philosophie than of sober mathematics, could only serve to dis-
courage further inquiry and interest in that direction. Thus wo
find that even the best treatises on botany and zoology abandon
the subject, satisfied with merely contrasting the simple geometrical
ground-forms of crystals with the highly curved and hopelessly
complicated lines and surfaces of the organism.
But there are other considerations which lead np to a mathe-
matical conception of organic form, those namely of symmetry and
regularity. These, however, are usually but little developed,
botanists since Schleiden contenting themselves with throwing
organisms into three groups— first, absolute or regular ; second,
regular and radiate ; third, symmetrical bilaterally or zj-gomorphic
—the last being capable of division into two halves only in a single
plane, the second in two or more planes, the first in none at all.
Burraeister, and more fully Bronn, introduced the fundamental
improvement of defining the mathematical forms they sought not
by the surfaces but by axes and their poles ; and Haeckel has
developed the subject with an elaborateness of detail and nomen-
clature which seems unfortunately to have impeded its study and
acceptance, but of which the main results may, with slight varia-
tions chiefly due to Jiiger {Lehrb. d. ZooL, i. 283), be briefly out-
lined.
A. ANAXONIA— forms destitute of axes, and consequently
wholly irregular in form, e.g., Amcebfe and many Sponges?
B. ^JTOJV/^— forms with definite axes.
I See Haeclcel, Gen. Marjih. L, KaOcaihrcammt 1., and Jtjui. Zutxhr. x. ; alad
Sachs, GtschichU d. Bot. ; Fisch, Av/sdhiung ti. Krilik, Ac, Rostock, ISiO;
Perrier, La Colonies AnimaUe, 1892, as from these aU other references can be
obtained.
s The sciences of organic and mineral form would thQs(Af Hacchel point*
out) become thoroughly analogous, for, as promorphology dcve)ot,s tlic crystallo-
graphyof organic form, so mineraiogy.in the studyof such phenomena as thoao
-otfisetidcaiorphisffl or et mineial development^ becomes parallel to morpbologjj
844
MORPHOLOGY
I. HoMAXONiA— all axes equal.
(o) SphJTCS, whore an indefinite number of equal area can
ba drawn through the middle point, e.g.^ Sphnrozoum.
(6) r olyhedra, with a definite number of like axes.
Of theso a cousiderable number occur in nature, for example, many
Radiolarians (fig. 3), pollen -grains, &c.,
and they are again classifiable by the
number and regularity of their faces,
II. Protaxokia, where all the parts
are arranged round a main axi3, and of
these we distinguish—
1. Mo7Uizonui,'^'it]\ not more than one
definite azis. Here are distipgiushed
(a) those with similar poles, spheroid
(Coccodiscus) and cylinder (Pyrosoma)
and (6) those with dissimilar poles,
cone (Conulina).
2. Sfauraxonia, wbere, besiJoa the j.^^ 5. - Hadiolarian (Etbmo-
main axes, a definite number of second- aphtera), an irrcf:uUr ondo-
ary axes are placed at right angles, and Bphseric polyhedron with equi-
the stereometric ground-form becomes aognlar faces. Type of Horn-
a pyramid. Here, again, may be distin-
guislied (a) those with poles similar, Stauraxonia komopola, where
the s<»creometric form is the double pyramid (fig. 4), and (&) those with
poles dissimilar, Stauraxonia heterO'
pota, where the stereometric form is the
eiiiflle pyramid, and where we distin-
guish a iJasal, usually oral, pole from an
apical, aboral, or anal pole. The 'bases
of these may be either regular or irre-
gular polygons, and thus a new classi-
fication into Homostauya and Iletero-
staura naturally arises.
The simpler group, the Homostaura, .j
may have either an even or an odd (r
number of eides, and thus among the
Homostaura we have even-sided and
odd-sided, single and double pjTamids,
In those Homostaura with an even
number of Eidca, such as Medusa;, the
radial and inter-radial asps have simi-
lar poles ; but in the series with an
odd number of sides, like most Echi-
noderras, each of the transverse axes is
half radial and, half semi-radial (fig. 5).
Of the group of regular double Vy^^-VioA.--Po\\2ri^lV:^s^\onno^iT^,
mids the twelve-sided poUen-gi-ain of as cjcample of Stanraxonia ho-
Passiflora (fig. 4) may be takeu as an mopola. Gronnd-fonn a regu-
example, having the ground-fonn of lar double pyramid 01 six sidea.
the hexagonal system, the hexagonal dodecahedron. Of the equal
even-sided single pyramids (Heteropola homostaura), Alcyonium,
Geryonia, Aurelia may be taken as ex-
amples of the eight-sided, aix-sided, and
four-sided pyramids, while those with an
odd number of sides may be illustrated
by Ophiura or Primula rnth five sides,
and tne flower of Lily or Rush with three
aides.
In the highest and most complicated
group, the Heterostaura, the basal poly-
eon is no longer ro^ar but amphithect
{6.y.(plOT]KTo% ~ double-edged). Such a
polygon has an even number of sides, and ^^__ „.—«„.„„„ ..^ ^^,^, „
can be divided into symmetrical halves * 'of Heteropola' bornostaam
by each of two planes intersecting at right Ground-form a re^ula.- sinjs-le
angles in the middle point, and thus divid- VJrs.mi^ of Ave aides,
ing tho whole figure into four congruent polygons. The longer of
these axes may be termed lateral, the shorter the equatorial ordorso-
ventral ; and those two axes, along with the main axes, always define
tho threedimensions of space. Ctenophores (fig. 6} famish examples
of ei^ht-sided amphithect pyramids, some Madrepore Corals of six-
eided, Crucifers, some MedusEe, and Cestodes of four-sided amphi-
thect pyramids.
In these forms tho poles of the dorso-ventral and lateral axes are
similar, and, as in the precuding Monaxonia and Stauraxonia, tho
centre of the body is defined by a line ; and they are therefore termed
Ceniraxonia, while the Protaxonia, which are defined by their cMitral
point, are- called Ccntrostigma. There are, however, other forms,
and those the most complicated, in which tho poles of at least the
dorso-ventral axis are unlike, and in which tho oody is thus defined
not with reference to a liuc but to a median plane, and these have
accordingly received the name of Ccntropipcda. Their ground-form
is a polygon with an uven number of sides, which can only bo
divided into two symmetrical halves by the one median plane. It
con be obtained by halvinj^ an amphithect pyramid of double tho
number of sides, and is consequently termed a half amphitliect
pyramid (fit;. 7). The whole amphithect pyramid may be moat con-
' Fio. 5.— Starflab, au example
veniontly obtained by the reduplication of the ground-form as if (n »
mirror. Of half amphithect pyramids therb are again two forma,
termed by Haeckel Amphipleura and ZygopUura, the former in-
cluding the "bilaterally symmetrical" or irregularly r&diate forma
of previous authors, such aa fipatangus, Viola, Orchis, while the
Zygopleura include forms bilaterally symmetrical in the strictest
sense, in which not more than two radial planes, and these at right
Fig. 6. Fig. 7.
Fio. 6.— Ctenophore (Eucharis). Grotud-form aaei^bvgided double amphithect
pyramid.
Fio. 7.— Spatangua. Ground-form a five-aided half amphithect pyramid,
angles to each other, are present. The stereometric ground-form
is a half rhombic pyramid. Haeckel again divides these, according
to the number of antimeres, into TelrapUura and DipUura,
Promorphology has thus shown that the reigning dogma of the
fundamental dSleronce of organic and mineral forma is false, and
that a crystallography of organic forms is possible, — the form of
the cell or the cell-aggregate difiering from the crystal merely by
its more or less \'L'5C0ua state of aggregation, its inherited peculi-
arities, and its greater adaptability to tho environment. The
Classification into bilateral and radiate forms which usually does
duty for more precise promorphological conceptions must be aban-
doned as hopelessly confusing essentially different forms, or at least
must be rigidly restricted, — the term radial to regular and double
pyramids, the term bilateral to the Centropipeda if not indeed to
dipleural forms. Similarly, the topographical and relative terms,
anterior and posterior, upper and under, horizontal and vertical,
must be superseded by the terms above applied to the axes and
their poles, oral and aboral, dorsal and ventral, right and left.
§ 6. Nature 0/ Morphological Changes. — The main forms of organic
structure being analysed and classified and their stage of individu-
ality being ascertained, the question next arises, by w'hat morpho-
logical changes have they arisen, and into what Categories can these
modes of difterentiation be grouped ? They at first sight seem
innumerable, yet in reality aie few. Goethe somewhat vaguely
generalized Ihem for the flower as ascending and descending Ineta-
morphosia, expanyicm and contraction of organs, kc. ; but the first
attempt at careful enumeration seems to be that of Auguste de St-
Hilaire, who recognised dofects of development, adhrrences, excesses
of production or "d^doublements," metamorphosis and displace-
ment of organs. Subsequent authors have variously treated the
subject ; thus Asa Gray enumerates as modifications of the flower —
coalescence, adnation, irregularity, abortion, tion-alternation or
anteposition, multiplication, enation, unusual development of the
axis, and other morphological modifications ccmiected with fertili-
zation. These are obvioi\sly lio numerous, as may best be shown
by a singlo comparison with the view of an animal morphologist.
Thus iiiixloy, in discussing tho arrangement of the Vortcbrata,
recognizes only three pro.x-jSfs of modification, not only in. tilie
ancestral evolution of the Equidoe, but in the 'indivi^luil de'."elop-
jnent of animals generally ; these are "(1) excess of development
of some parts in relation to others, (2) partial or complete suppres-
sion of certain parts, (3) coalescence of parts originally distinct."
It is probable that this " threefold lav/ of evolution " may include
all observed casc5 ofchangc, even in the Cower ; thus Chorisia and
Peloria may bo regarded aa pocuU?.r forms of excess, while displace-
ment is probably in all cases only apparent, and really duo to
adhesion or coalescence (see Biolotx", vol. iii. p. 6Si sq.).^
§ 7. Nature 0/ Morp/whgical Correspondtncc — Categories cf
Homology. — To indicate all the steps by which the idea of mor-
phological has been distinguished from that of physiological
resemblance would be to examine the whole history of morphology;
it must suffice to discuss the terniinology of the subject which has,
as ever, served not only as an index but as an engine of progress.
For these two distinct forms of resemblance tho terras houwiogy
ami analogy gradually became specialized, and ^vere finally estab-
lished and clearly defined by Owen in 1S43, — "tho former as the
same organ in different animals under every variety of form and
function (c.j., fore-limbs of Driito volarts and wings of Bird) : the
second as a part or organ in one animal which has the same function
» Conipnro A. do St-HUalrc, Morp}.,.loffie ; Gray, J/auwuL p. 179 (1S^>;
Suxlejr, rrix. Zool, Society, p. 619, Load., 1880,
MOBPHOLOG\
845
SI acotliei part or argan » a different inunal {e.g. , parachute of
Praco and wings of Bird). He farther distinguiehea three kinds
of homology ; — (1) specuil, being ** that above defined, namely, the
correspondence of a part or organ determined by its relative position
and connexions with a part or organ in a diflerent animal, the
determination of which homology indicates that such animals are'
constituted 'on a common type, ' e.g.f basilar process of human
occipital with basi-occipital of fish; (2) general, that "higher
relation in which a part or series of parts stands to the fiindamental
or general type, involviBg a knowledge of the typo on which the
group in question is constituted," eg., the same human bone and
centrum of the last cranial Tertebra ; (3) scria( homology, ' ' repre-
aentative or repetitive relation in the segments of the same skeleton "
(demonstrated when genwal and special homologies have been
determined) ; thTis usually the basi-occipital and basi-sphenoid
are *'homotypes." These terms were nenceforth accepted by
naturalists ; but the criterion of analogy and homology became
for Agassi: and other embryologists developmental as well as
comparative, reference to the ideal archetype becoming less
and less frequent Passing over the discussions of Agassiz and
Bronn, of wnich the latter is criticized and partly incorporated
by Haeckel, we find the last-named (1) placing serial under general
homology ; (2) erecting categories of homology partially corre-
sponding to those of individuality, — (a) homotypy (of antimeres),
hence distinct from that of Owen, (6) hmwdynavty (of metameres),
(c) hotaorurmy (of parts arranged on transverse axes) ; (3) defining
special homology in terms of identity of embryonic origin. In
1870 this latter point- was more fully insisted upon by Ray Lan-
kester, who, decomposing it into two others, proposed to supersede
the term homology by kojnogeny, being the correspondence of
common descent, and homoplasy, denoting any superinduced
correspondence of position and structure in parts eraoryonically
distinct. Thus, the fore-limb of a mammal is- hoTJwgcnous with
that of a bird, but the right and left ventricles of the heart in
both are only homoplastic, these having arisen independently since
the divergence of both groups from a xmi-ventricuiato ancestor in
relation to similarity of physiological needs. Mivart next pro-
posed to retain homology as a generic term, with homogeny and
homoplasy as two species under it, and carried the analysis into
Seat detail, distinguishing at first twenty-five, but later fifteen,
nds of correspondeuce : — (1) parts similar in function only, e.g.,
legs of Lizard and Lobster ; (2) parts similar both in function and
relative position, vrings of Bat and Bird ; (3) paits of common
descent, fore-limb of Horse and Rhinoceros ; (4) parts of similar
embryonic origin, whatever be their racial genetic relations, e.g.,
occipitals of Panther jtnd Perch ; (6) parts of dissimilar embryonic
origm, whatever be their racial genetic relations, e.g., legs of
Diptera; (6, 7, 8, 9, 10) laterally, vertically, serially, antero-
posteriorly, and radially homologoos parts; (11) subordinate
w;rial homologucs, e.g., joints of antenna ; (12 and 13) secondary
and tertiary subordinate serial homologues ; (14 and 15) special
and general homologies (in Owen's sense). In his Kalkschwdrmme
Haeckel proposed to term Iwnujphyly the truly phylogenetic
homology in opposition to homomorphy, to which genealogic basis
is wanting ; and finally Von Jhering bias pubUshed a r«pctitian of
Lankester's view.
In this discussion, as in that of individuality, it is evident that
wo are dealing with numerous logical cross-divisions largely corre-
sponding, no doubt, to the complex web of inter-relations presented
by nature, yet remaining in need of disentanglement. Though we
must set aside analogies of functional activity, the resemblances
in external shape or geometric ground-form wliich correspond to
these, e.g., Hydrozoa and Bryozoa, Fishes and Cetaceans, mimetic
organisms, are nevertheless, as our historic survey showed, the
first which attract attention ; and these homoplastic or homomor-
phic forms, as Haeckel has shown, come as fairly within the province
of the promorphologist as do isomorphic crystals within that of
his an-organological coUeaguo the crystallogi-apber. Here, too,
wojild be considered "radikl," "vertical," "lateral" homology,
" homotypy of autimews," and all questions of symmetry, for which
Haeckel's nomenclature oiliomasconial, Jiomopolic, kc, is distinctly
preferable. Entering the field of tectology or morphology in the
ordinary sense, we vaay next consider whether two organisms com-
pared are of the same category of individuality — are homocalcgoric ',
and under this seiial homology, for instance, would come as a
minor division, the correspondence between the units or parts of
units of a linear dyad-deme or triad. From a third point of view,
that of the embryologist, we trace the development of "each multi-
cellular organism (1) from the embiyonic layers and systems into
which the secondary unit (gastnila or plant embryo) differentiates,
(2) from a unit-demo or unit of the inferior order or orders of
individuality. The parts and units thus recognized by ontogenetic
i-escarch, respectively or successively homodermic, homosystemic,
and homodeniic, may then conveniently be termed (indifferently
aavo for considerations of priority) either "specially homologous,"
" homogenous," " homophylic," or "homogenetic," in the language
of phylogenetic theory. These three great classes of morphological ,
correspondence — promorphological, t«otological, and embtyclogical
—may or may noc coincide. But the completest homology,
in which all forms of resemblance unite and from which they
differentiate, is that expressed in the cell theory, or rather in that
ovum theory which underlies it, and which Agassi2 therefore not
unjustly retarded as " the greatest discovery in the natural sciences
of modem timea " >
S 8. Baulta to Taxonomy. — The advance and modification of
classifications which follow each morphological advance have been
pointed out above, and taxononiy thus never quite reaches a level
with morphological knowledge. That it requires much reform tct
present is obvious. Although the dogma of the constancy of species
is no longer maintained, its results survive, and perhaps a majority
of groups have still to be remonographed in the generalizing spirit
with which Haeckel has treated the calcareous Sponges, or Car-
penter, Parker, and Brady the Foraminifera. The union of the
Protophjrta and Protozoa into the Protista (a generalization which
research is constantly confirming) involves a final abandonment of
the mediaeval figment of three kingdoms of nature, and a revival of
the Organisata of Linnaeus. Physiological prejudices, too, are not
completely expelled ; bence, for instance, the constant attempts
■to separate Animalia and 'V'egetabilia by physiological character-
istics, which would be irrelevant even if in themselves valid. A
strictly morphological standard mnst be applied to the constmction
of classifications and the pruning of genealogical trees ; organisms
are " higher'" or "lower ' not according to their stage of evolution
in beauty or intelligence but (as Huxley has most clearly pointed
out in the essay referred to under § 6) to the degree of morphological
differentiation by excesa, suppression, or coalescence wnich they
exhibit. Thus the supreme position of Man in classification must
be abandoned, since the Primates are simply one of the less special-
ized, i.e., lower orders of Mammals, and the Mammals themselves
are on the whole distinctly less specialized than the Birds, or per-
haps even some of the higher Reptiles. The morphological import-
ance of the "vegetable kingdom" sinks when tested by such a
standard. The Cormophyces are all nothing more than an axis
with appendages, and as such may fairly be compared, not with
the entire animal assemblage, but merely to that group which is
homomorphic (or rather isomorphic) with them as reducible to
axis and appendages too. Such a gronp we find in the Hydiome-
dusffi, which we can easily model in imagination into all the special-
izations of the floral world, a single genus like Clava or Tubularia
affording a starting-point for countless "natural orders."
§ 9. Selation 'of MorpMogy to Physiology. — Although the pure
morphologist investigates laws of structure only, and rightly elimi-
nates the conceptions of life, envii-onraent, and function, yet if kept
permanently apart from physiological considerations h's labours
would b« incomplete and his results inexplicable, if not indeed
almost illusory. For, however deeply one penetrates through super-
ficial and adaptive characters to an apparently permanent and
fundamental morphological type, this is itself but an earlier adapta-
tion, showing the fading traces of an earlier adaptation stilL And,
conversely, the most superficial of adaptive characters, if trans-
mitted to numerous varying descendants, may attain high morpho-
logical importance. The morphological aspect of an organism is
merely statical, and, like that of an eddy or a vortex-ring, becomes
only truly intelligible when viewed in its dynamic aspect ; and
thus, though the demonstration of the structural unity of the
organic world is in itself a great result, yet the desire of a deeper
explanation of form as determined by function and environment
is thereby rendered all the more pressing. An example may be
taken from botany. Thus Airy beautifully explains the pheno-
mena of phyllotaxis as adaptations to bud-life. Or again, in a
common flower, say the Dead-nettle, all the details of form are in-
deed described by the eystematist with equal minuteness (a pro-
ceeding which, except in so far as serving for specific identification,
is of no fmther scientific value), but receive separate interpretation
from the two distinct standpoints of the morphologist and physio-
logist. The latter, to whom form is. important merely so far as
explanatory of function, shows how the tough persistent calyx is
protective against various dangei-s, how the corolla-serves to lure
the fertilizing bees, which find in its lip a landing stage and in
each lateral process a hold-fast, while its hood at once protects the
pollen against rain and determines the curvature of the stamens, —
this curvature, as well as their didynamous arrangement, median
position, and linearly arranged anther-lobes being all adaptations
through the medium of the bee's hairy back to meet the similarly
placed stigma of another flower, — and so on. The morphologist,
on the other hand, analyses the calyx into its five constituent sepals,
reduces the corolla to a regular pentamerous tj-pc, ascertains the
position of the four stameus, and asserts the loss of a fifth posterior
one, finds the ovary to bo primitively two-celled, and thus reaches
a sdiematic conception of a not archetypal but ancestral fomi.
This ground-form itself, however, suggests a new train of considera-
tions both morphological and physiologic^d respecting the origin of
Lookester, An. Mag. Nat. Hist., 1870, or. Oeddes,
846
M O R— -M O R
this priincA'al flower ftoni a somewhat fem-like Cryptogam, of which
tiie foliagc-lcftves, the envelopes of the sporc-bcai-ing leaves, the
micro- and raacrosporangiosphores had become permanently difTer-
«ntiated in ascending order ; of which the microspores, doubtless
through the intervention of a spore-eating insect, had come to ger-
minate upon the macrosporangium instead of upon tile gl-ound ; and
in which this variation (evidently advantageous, since making ferti-
lization at once more certain and more economical) was aided to per-
petuate itself by the contemporaneous evolution of those floral colours
which are nascent even among the Thallophy tes. Ami thus the mor-
phologist, though excluding telcological and functional considera-
tions from his anatomical researches, has yet a physiological ideal,
and enters sooner or later upon a new series of inquiries — those of the
interdependence of structure and function. Milne-Edwards's law of
the physiological division of labour, Dohrn's principle of functional
change, the speculations of Claude Bernard, Spencer, and Hacckel,
cxp'-'riMicntal inquiries such as those of Semper, where organisms
arc subjected to special modifications of their environment, and
the like, arc all contiibutions to this newest and evolutionary
department of morphology. Such ideas aro even ajipliod to the
study of celUdar morphology. Thus, Spencer points out the relation
of the shapes of cells to their environments ; James ingeniously
explains tho occuiTence of cell-division by the rapid increase of
bulk over surface which the growth of a solid involves, and the
corresponding increase of dilficulty of nutrition ; and the writer
has attempted to explain the forms of free and united cells as
specializations of a (protomyxoid) cycle in wliicli variations of func-
tional activity are accompanied by the assumption of corresponding
forms, the whole series of changes depending upon the properties
of protoplasm under the variations in the supply of energy from
the environment. Rauber, His, and others have even attempted to
explain einbryological phenomena in terms of the "simplest cellular
mechanics, but as yet such speculations are somewhat crude.*
§ 10. Oricniaiion mid Subdivisions of Morphology. — The position
of morphology in the classification of the sciences and the proper
mode of subdividing it cannot be discussed within these limits,
although tho latter is especially the subject of much disagreement.
The position above assumed, that of including under morphology
the whole statical aspects of the organic world, j^ that of Haeckel,
Spenoer, Huxley, and most recent animal morphologists ; botanists
frequently, however, still use the term under its earlier and more
limited significance.^ (P. GE.)
MORRIS, RoEEKT (1734-1806), American statesman,
v.-as born at Liverpool, England, on 20th January 1734.
At the age of thirteen he accompanied his father to America,
and after serving in a counting-house at Philadelphia
he became in 1754 partner in the business. From 1776
to 177S he was delegate to the Continental Congress, and
he vas one of those who signed the Declaration of Inde-
pendence. During the war he served on the committee of
M'ays and means, and freely placed his immense wealth at
the disposal of his country, his personal credit being at
one time pledged to the amount of 811,400,000. He also
in 1780 established the Bank of North America, and until
1784 acted as superintendent of finance. In 1786 he be-
came a member of the Pennsylvania legislature, and he was
one of the convention which framed the Federal constitu-
tion in 1787. From 1786 to 1795 he was United States
senator. On account of the disastrous result of some of
his financial speculations Morris passed the later years of
his life in a debt prison. He died at Philadelphia, 8th
May 1806. Robert Morris had as his assistant-superin-
tendent of finance Gouverneur Morris (1752-1816), with
whom he engaged also in several mercantile enterprises.
Gouverneur MoitIs, who rose to some eminence as a states-
man and orator, was more fortunate ia his speculations
than his colleague, and latterly became celebrated for the
munificence of his hospitality. He was the author of a
series of essays on currency and finance, which are included
iiT the Life, Currespondence, and ]]'ritin<js of Gouverneur
Morris, 3 vols., edited by Jared Sparks, 1832.
MOKRIS-D.ANCE, or ■Morkice-dance, a performance
for a long time associated with certain festive seasons in
England, but now wholly discontinued. The origin of the
name is doubtful ; and whethev the dance was indigenous
to England, or was introduced by John of Gaunt from
Spain, or was borrowed from the French or Flemings,
must be left to conjecture. That, as the name would
seem to indicate, it was a development of the morisco-
(lance or Spanish fandango is not, however, invalidated
by the fact that the morisco was for one person only, for,
although latterly the morris-dance was represented by
\.irious characters, uniformity in this respect was not
always observed, and tho elements of the dance may have
been borro^^■ed from the morisco. There are few references
to it earlier than the reign of Henry VII., but it would
appear that in the reign of Henry VIII. it wa.s an almost
essential part of the principal village festivities. Although
allusions to it in poems are very frequent in the 16th and
17th centuries;, nothing more than fragmentary descriptions
have been handed do-\vn to us, so that an accurate know-
ledge of its characteristic features at even any particular
period is impossible. In earlier times it was usually
danced by five men and a boy dressed in a girl's habit,
who was called Maid Marian. There were also two
musicians ; and, at least sometimes, one of the dancers,
niore gaily and richly dressed than the others, acted as
"foreman of the morris." The garments of the dancers
were ornamented with bells tuned to different notes so as to
sound in harmony .^ Robin Hood, Friar Tuck, and Little
John were characters extraneous to the original dance,
and were introduced when it came to be associated with
the May-games. At Betley, in Stafford-shire, there is a
painted window of the time of Henry VIII., or earlier,"
portraying the morris, — the characters including Maid
Marian, Friar Tuck, the hobby-horse, the piper, the tabotu-er,
the fool, and five other persons apparently representing
various ranks or callings. The hobby-horse, which, latterly
at least, was one of the principal characters of the dance,
consisted of a wooden figure attached to the person of the
actor, who was covered with trappings reaching to the
ground, so as to conceal his feet. The morris-dance was
abolished along "with the May-games and other festivities
by the Puritans, and, although revived at the Restoration,
the pageant gradually degenerated in character and declined
in importance. Maid Marian latterly was personated by
a clo^vn who was called Malkin. Though the dance is now
wholly discontinued, it is probable that some of the original
elements of it still survive in a country-dance which, under
the same name, is still popular in the north of England.
See Douce, *' Dissertations on the Ancient Jlorris Dance," in his
IlUislmtioiis of Shakspcare{\iW); Strutt, Sports and Pastimes of Uie
People of England ; and Brand, Popular Antiquities (1849).
MORRISON, Robert (1782-1834), the first Protestaflt
missionary to China, was born of Scottish parents .at
Morpeth, Northumberland, on 5th January 1782. -After
receiving an elementary education in Newcastle, he was
apprenticed to a lastmaker, but his spare houi-s weTB
devoted to studies connected with theology, and in 1803
he was received into the Independent academy at Hoxton.
I In tho following year he offered his services to the London
Missionary Society, by which, after ho had attended the
mission college of Gosport and studied Chinese under a
native teacher, he was sent to Canton in 1807. He was
appointed translator to the East India Company's factory
iples of Biol, ;
vie coinmmis
' See, Biology, vol. iii. p. C81 sq. ; Spencer,
Haeckel, Gen, Morph. '; C. Bernard, Phinominc
aux an. ei aux vig. ; Semper, Animal life ( 1 880) ; ' J.amea, Edini
iled. Journal, 1883 ; Geddcs, Zool. Ameiger, 1SS3 ; Rauber, ilorph.
ya/i)!)., vi. ; Hacckel, yrai'cscAioamiili;, i. p. -ISl, &c.
- See Haeckel, GH. Morph., i. Introduction ; also Comte, Phil^.
Pos., iii. (1851-1854) ; Spencer, Prin. of Biol., i. ; Gcgcnbaur, Comp:
Anat. ; Asa Gray, Manual; and tha article Bioloot ; also Geddej^
Jena Xcitschr., 1883.
' See Sir Walter Scott's Fair Maid of Perth, note on a drest pre-
served by the glover incoruoration of Perth.**
M O R — M O K
847
there in 1808, and, in addition to his official duties con-
nected -with this post, labourad with intense "^application
Bt a Chinese Grammar ,and a translation of the New
Testament, both of which were published "in 1814. In
1817 he published A View of China for Philological Pur-
poses, and his translation of the entire Bible was completed
in the following year. Hia next enterprise was the estab-
lishment of an Anglo-Chinese college at Malacca for " the
reciprocal cultivation of Chinese and European literature,"
which was opened in 1820. In 1821 his Chinese Dictionary
was published by the East India Company at an expense
of £15,000. Leaving China at the close of 1823 he spent
two years in England, where he advocated Chinese missions
before large and enthusiastic audiences, and was elected a
Fellow of the Royal Society. Returning to China in 1826
he set himself to promote education and to prepare a
Chinese sommentaiy on the Bible and other Christian
literature. He died at Canton on 1st August 1834. His
ifemoirs, compiled by his widow, were published in 1839
(2 vols. 8vo, London).
MORRISTOWN, a city of the United States, county
seat of Morris county. New Jersey, lies on the Whippany
river, 31 miles from New York by the Morris and Essex
division of the Delaware, Lackawanna, and Western Rail-
road. It was twice the headquarters of the American
army during the War of Independence, and Washington's
residence, owned by the Washington Association, assisted
by the State, is a half-mile to the east. On Whatnong
mountain, 3 miles distant, stands the State insane asylum,
usually called Morristown Asylum, a vast granite building
1243 feet long, erected in 1874-1875, and capable of ac-
commodating 1000 patients. The population in 1880
was 5418.
MORSE, SAjotel Tmisv Brekse (1791-1872), artist
and inventor, was bom at the foot of Breed's Hill, Charles-
town, Massachusetts, on 27th April 1791. His father was
the Rev. Jedediah Morse, D.D., the author of Morse's
Geography. At the age of fourteen Samuel Morse entered
Yale College ; under the instruction of Professors Day and
Silliman he received the first impulse towards those elec-
trical studies with which his name is mainly identified.
In 1811 Morse, whose tastes during his early years led
him more strongly towards art than towards science, be-
came the pupQ of Washington Allston, then the greatest of
American artists, and accompanied his master to England,
where he remained four years. His success at this period
was considerable; but on his return to America in 1815
he failed to obtain commissions for historical paintings,
and after working on portraits for two years at Charleston,
S.C, he removed first to Washington and afterwards to
Albany, finally settling in New York. In 1825 he laid
the foundations of the National Academy of Design, and
was elected its first president, an office which he filled
until 1845. The year 1827 marks the revival of Morse's
interest in electricity. It was at that time that he learned
from Professor J. F. Dana of Columbia College the ele-
mentary facts of electromagnetism. As yet, however, he
was devoted to his art, and in 1829 he again went to
Europe to study the old masters.
The year of his return, 1832, may be said to close the
period of his artistic, and to open that of his scientific life.
On board the packet-ship "Sully," which sailed from
Ha\Ta 1st October 1832, while discussing one day with
his fellow-passengers the properties of the electromagnet,
h« was led to remark : " if the presence of electricity can
be made visible in any part of the circuit, I see no reason
why intelligence may not be transmitted by electricity."
It was not a novel proposition, but the process of formu-
lating it started in his mind a train of new and momentous
ideas. The current of electricity, he knew, would pass
instantaneously any distance along a wire ; and if it wore
interrupted a spark would appear. It now occurred
to him that the spark might represent a part of speech,
either a letter or a number ; the absence of the spark,
another part ; and the duration of its absence, or of the
spark itself, a third, so that an alphabet might be easily
formed, and words indicated. In a few days he had
completed rough drafts of the necessary apparatus, which
he displayed to his fellow-passengers.* During the twelve
years that followed Morse was engaged in a painful struggle
to perfect his invention and secure for it a proper presenta-
tion to the public. The refusal of the Government to com-
mission him to paint one of the great historical pictures in
the rotunda of the Capitol seemed to destroy all his old
artistic ambition. In poverty he pursued his new enter-
prise, making his own models, moulds, and castings, deny^
ing himself the common necessaries of life and encountering
embarrassments and delays of the most disheartening kini
It was not until 1836 that he completed any apparatus
that would work, his original idea having been supple-
mented by his discovery in 1835 of the " relay," by means
of which the electric current might be reinforced or renewed
where it became weak through distance from its source.
Finally, on 2d September 1837, the instrument was
exhibited to a few friends at his room in the university
building. New York, where a circuit of 1700 feet of copper
wire had been set up, with such satisfactory results as to
awaken the practical interest of the Messrs Vail, iron and
brass workers in New Jersey, who thenceforth became asso-
ciated with Morse in his undertaking. Morse's petition
for a patent was dated 28th September 1837, and was
soon followed by a petition to Congress for an appro-
priation to defray the expense of subjecting the telegraph
to actual experiment over a length sufficient to estabUsh
its feasibility and dentonstrate its value. The committee
on commerce, to whom the petition was referred, reported
favourably. Congress, however, adjourned without making
the appropriation, and meanwhile Morse sailed for Europe
to take out patents there. The trip was not a success.
In England his application was refused, on the alleged
ground that his invention had been already published;
and, while he obtained a patent in France, it was subse-
quently appropriated by the French Government without
compensation to himself. His negotiations also with Russia
proved futile, and after a year's absence he returned to
New York. On 23d February 1843 Congress pa.ssed the
long-delayed appropriation, steps were at once taken to
construct a telegraph from Baltimore to Washington, and
on the 24th of May 1844 it was used for the first time.
Morse's patents were already secured to him and his asso-
ciates, and companies were soon formed for the erection of
telegraph lines all over the United States. In the year
1847 Morse was compeUed to defend his invention in tho
courts, and successfully vindicated his claim to be called
the original inventor of the electromagnetic recording tele-
graph. Thenceforward Morse's life was spent in witnessing
the growth of his enterprise and in gathering the honours
which an appreciative public bestowed upon him. As
years went by he received from the various foreign Govern-
ments their highest distinctions, while in 1858 the repre-
sentatives of Austria, Belgium, France, the Netherlands,
Piedmont, Russia, the Holy See, Sweden, Tuscany, and
Turkey appropriated the sum of 400,000 francs in recog-
nition of the use of his instruments in those countries. In
the preparations for laying tho first Atlantic cable he took
an active part, though the attempt of 1857, in which he
personally engaged, was not successful He died 2d April
* Five years later the captain of the ship identiOed under oath
Morse's completed instrament with that which Mor^o had explained
on boiird the " Snlly " in 18S2.
848
M O R — M O R
1 872, at New York, where his statue in bronze now stands
in the Central Park. His instrument and alphabet are
DOW used on 95 per cent, of the telegraph wires of the
world. (s. L P.)
MORSHANSK, a district town of Russia, situated in
the government of Tamboff, 58 miles (187 miles by rail)
to the north of the capital of the province on the Tsna
river, a tributary of the Oka, and on the railway between
Moscow and Orenburg. The village Morsha was founded
only in the middle of the 17th century, and received
municipal institutions in 1779 ; but a hundred years ago it
was already a wealthy town, owing to its situation in a
most fertile district. Since it was brought into railway
communication ^vith Riazhsk (on the railway between
Moscow and Riazan) it has acquired still more importance,
and has become the chief centre for trade in wheat raised
ia the governments of Tamboft", Penza, SaratofiF, and in the
eastern districts of the government of Riazan. Merchants
from Moscow, Yaroslav, Yladimir, St Petersburg, and the
Baltic ports come t,o Morshansk to make large purchases
of grain, flour, hemp-seed, tallow, and potash. These are
seat, either to the Shilovskaya loading-place, or by rail to
Moscow. There are in Morshansk several steam flour-
mills, distilleries, and large store-houses for grain ; the
town, though built of wood, is cleaner than most of the
towns of the black-earth region. Morshansk has also some
importance for the import of manufactured ware brought
from the north and sent thence to the villages of the neigh-
bouring districts. Population, 20,000.
MORTALITY TABLES. See Insueance, vol xiii. p.
169 s?.
MORTGAGE. The general object of mortgage is to
secure a money debt by making it a charge on land, so that,
if the debt be not paid by a time agi-eed upon between the
parties, the creditor may sell the land and pay himself
out of the proceeds. In English law this is done by a
conveyance of the land in absolute terms to the creditor,
subject only to its being defeated if the debt should be
paid at the time fixed — an arrangement to which the law
has attached peculiar incidents designed to carry out its
real object. An absolute conveyance, however, is by no
means essential to the purposes of mortgage.
The histoiy of mortgage transactions in Roman law
shows three well -marked stages. In the beginning the
estate was conveyed absolutely to the creditor, who made
a covenant {fiducia) to reconvey it when the debt should
be paid. All the interest, however, in the meantime passed
from the debtor to the creditor, and should the latter
refuse to reconvey there was no remedy to the original
owner except a personal action. In the second stage
(that of piffnus) the property did not pass to the creditor ;
he merely received possession of the thing pledged, together
with certain rights of sale, &c., in the event of payment not
being m.ade at the time appointed. Lastly, without part-
ing with the possession even of the pledge the debtor
could create a hen or charge {kypotheca) over it in favour
of the creditor, who acquired thereby a right on failure
of payment to follow the thing by real action against the
possessor, whosoever he might be, and to repay himself
from the proceeds of his sale.
The mortgage of English law is the result of two dis-
tinct influences. Its origin and form belong to the common
law ; the restrictions by which it is made to serve the
purpose of a security only, and nothing more, belong to the
courts of equity. In the eye of the common law the
mortgagee was the o-ivner of the estate conveyed in the
mortgage ; in equity the mortgager remains the real owner,
and the mortgagee is merely an encumbrancer. A, the
owner of land m freehold, conveys to B and his heirs, with
a proviso that on repayment of money lent by B to A, on
a future day, with interest until payment, B or lib hfirs
will reconvey the estate to A and his heiri^, and that, until
default be made in payment, A and his heirs may hold
without interruption from B and his heirs. This is a
common mortgage of land, and at law, after failure of
payment, the land belonged absolutely to the mortgagee,
while in the meantime, before payment, the legal estate
was considered to be vested in him, subject only to being
defeated by payment at the proper time. The Court of
Chancery first interfered in the reign of James L to decree
a redemption after forfeiture, and a case in the reigTi of
Charles I. decides that payment after forfeiture has the
same effect as payment before. The right of the mort-
gager to redeem his estate after it has been forfeited,
according to the terms of the deed, is called his equity c'
redemption. No agreement between the parties was suffered
to oust the jurisdiction of the court, or to deprive thf
debtor of his equity of redemption. And this equity, at
first regarded as a mere right of the debtor, became
estabhshed in course of time as an estate in land which
descended to the heirs of the mortgager. On the other
hand, the interest of the mortgagee is part of his personal
estate, and passes to his executor and not to his heir. In
spite of the terms of the mortgage, the owner of the land
is still the owner, and the mortgagee is a creditor for the
money he advanced and the interest thereon. It may be
a question whether a given deed is a conveyance or a
mortgage, and the court, in deciding, will look at all the
circumstances of the case, and will treat it as a mortgage
when it was the real intention of the parties that it should
operate as a security only. Thus, if the price was grossly
inadequate, if the purchaser was not let into immediate pos-
session, if he accounted for the rents to the grantor, retaining
an amoimt equivalent to interest, if the expense of the
deed was borne by the grantor, there would be reason to
believe that the conveyance was only meant to be a mort-
gage. And " once a mortgage, always a mortgage ; " no
subsequent agreements can change its character.
A mortgagee may, however, on default of payment file
a bill of foreclosure requiring the mortgager to pay the
amoiuat of the debt with interests or costs by an appointed
day, or submit to be deprived of his equity of redemption.
The effect of failure to pay by the time appointed would
be to make the mortgagee absolute owner of the estate ;
but the court in any foreclosure suit may, at the request
of either side, order a sale 'instead of a foreclosure. And
a power of sale is now implied as one of the incidents of
the mortgage, imless forbidden or varied by express des-
tination. The mortgagee is entitled to retain out of the
proceeds of the sale the amount of his principal, interest,
and costs, the surplus belonging to the mortgager. A
mortgager cannot require the creditor to receive payment
before the time appointed in the deed ; and, on default of
payment at the appointed time, he must give the creditor
six months' notice of his intention to pay off the mortgage,
so that the creditor may have time "to look out lor a
fresh security for his money."
When the same land is successively mortgaged to different
persons, their rights take priority according to their chrono-
logical order. But the operation of equitable doctrines
in the formation of the law of mortgage leads to an im-
portant modification of this rule. Of the successive mort-
gagees, the first only takes the legal estate, and this,
according to the maxim of the Court of Chancery, will
turn the scale when there is an equality of equitable rights
between two contracting parlies. Thus, if the third mort-
gagee had no notice at the time of making his advance of
the existence of the second mortgagee, the equities of the
two claimants are supposed to be equal, and if nothing
else inten'ened priority of time would decide the order of
0 R — M O S
849
thdr nghts. But if the third mortgagee gets an assign-
ment of the first mortgage, he can tack his third mortgage
to the first, and so postpone the second mortgagee. And
if tha first mortgagee himself makes an additional advance
after the date of the second mortgage, but without notice
of it, his whole debt will take precedence, of the second
mortgagee. A similar result of equitable rules is seen in
the consolidation of securities. Two separate estates,
mortgaged at different times and for -different sums of
money by the same mortgager to the same mortgagee, are
regarded as consolidated, so that the whole of the land
becomes security for the whole of the money, and the
owner cannot redeem either mortgage without redeeming
the other. So that, as Mr Justice Williams reasons, no
person can safely lend money on a second mortgage, for,
in addition to the risk of a third mortgagee tacking, there
is the danger that, if the mortgager should have mortgaged
another estate for more than its value, the holder of the
deficient security may buy in the first mortgage, consoli-
date it with his own, and exclude the second mortgagee.
An eqnitable mortgage is constituted simply by the
deposit of title-deeds in security for money advanced.
The enactment of the Statute of Frauds that no action shall
be brought on "any contract or sale of lands," (Sic, or any
interests in or concerning them unless the agreement be
in writing and signed by the party to be charged, has been
cited as incompatible with the recognition of equitable
mortgages, but it is argued by Lord Abinger that the Act
\va3 never meant to affect such a transaction. The deeds
which are the evidence of title could not be recovered in
an action at law, and, it they were claimed in equity, the
court would require the claimant to do equity by repaying
the money borrowed on the deposit. Any subsequent
legal mortgagee, having notice of the deposit, will be post-
poned to the equitable mortgagee, and when the legal
mortgagee has not inquired as to the title-deeds the court
will impute to him such knowledge as he would have
acquired if he had made inquiry
As to mortgages of personal property see Pledge.
United States. — In the United States there b great diversity in
the extent to which equitable principles have been formally substi-
tuted for the rules of the common law in dealing with mortgages.
Washburn (Law of Heal Property, vol. ii ) arranges the States into
three "pretty wel^- defined classes." In the first, the mortgage
deed is hold to create a seizin of ard ah estate in the premises, with
all its common law incidents, to be enforced if need be by eject-
ment. In the second, the mortgagee's rights are limited to such
as the roles of equity prescribe, and may not be enforced by a suit
at law. In tho third, the mortgagee's interest is not deemed an
estate at all, but is here only to be enforced by t)ie sale of the pre-
mises as a means of paying the debt. In tho first class come
Massachusetts, Maine, Connecticut, Kow Hampshire, Rhode Island,
Vermont, Indiana, Missouri, North Carolina, Mississippi, Minnesota ;
Sh the second, Iowa, Illinois, Pennsylvania, Kentucky, Ohio,
Wisconsin, and Texas ; in the third, Califomia, Georgia, and New
York, to Avhich may be added Oregon (K K.)
MORTIFICATION, a term used in surgery signifying
a local death. Any cause which interferes with the blood-
supply of a portion of the body will, if sufficiently pro-
longed or sufficiently severe, give rise to mortification. In
some cases the death may be preceded by inflammation ;
in others, as in old people with diseased vessels, the part
may die in consequence simply of insufficient blood-aupply
without any previous inflammation. The part is said to
mortify ; the process is termed gangrene ; the dead part is
called a slough. A severe injury may end in mortifica-
tion. Extreme heat as in severe burns, or extreme cold
as in frost-bite, may give rise to the condition. Those
parts of the body farthest from the centre of the circula-
tion are most liable to mortification. Frost-bite, for ex-
ample, may attack the toes or fingers as well aa those
parts which are most exposed to the cold, more particu-
larly the point of the nose or the ears. The part affected
lft-32
becomes pale, bloodleBS, cold, and insensible. The great
point to attend to is to restore the circulation gradually;
using gentle friction. If the person is brought before a
fire, or if any hot applicatioas are used, then a rapid re-
action may issue in a severe inflammation, which may be
followed by mortification. Chilblain is a mild form of
frOst-bite occurring in young people with sluggish circula-
tions, very often caused by sitting down before a strong
fire with cold feet ; any one suffering from cold feet or
hands should take plenty of exercise, and if after a return
from a sharp walk the feet remain cold the heat should bo
restored by rubbing with a rough towel.
MORTMAIN, Statutes of. The object and effect of
these enactments are treated in the articles Chaeitv and
CoEPOEAiioN (q.v.). The following is a list of the Mort-
main Acts : —
9 Henry III. c 36 (Magna Charta) ; 7 Edward I. st. 2, c. 1
(De Keligiosis) ; 13 Edward I. c. 82 ; 13 Edward I. c. 41 ; 18 Ed-
ward I. St. 1, c. 3 ; 27 Edward I. st. 2 ; 34 Edward I. st 3 ; 18
Edward III, st. 3, c. 3 ; 15 Richard II. c. 6 ; 21 Henry VIII. c. 6,
8. 5 ; 23 Henry VIII. c. 10 ; 1 and 2 Philip and Mary, c. 8, s. 51 ;
35 Elizabeth, e.' 4 ; 21 James I. c. 1 ; 13 and 14 Charles II. c 6,
s. 10 ; 29 Charles II. c. 8 ; 7 and 8 William III. c. 37j 9 George II.
c. 36 ; 43 George III. c. 108 ; 9 George IV. c. 85 : and 2 aiid $
William IV. c. 115.
MORTON, James Douglas, fourth earl of (1530-1581),
regent of Scotland, second son of Sir George Douglas of
Pittendriech, was bom at Dalkeith in 1530. Having
married Elizabeth, daughter of the third earl of Morton,
he through her succeeded in 1553 to the title and estates
of his father-in-law. After the return of Queen Mary in
1561 he was chosen a privy councillor, and in 1563 he
became lord high chancellor. Though his sympathies were
Protestant, he took no part in the combination of Protestant
barons in 1565, but he headed the armed force of 150 men
who took possession of Holyrood Palace to effect the assas-
sination of Eizzio, and it was to his house that the leading
conspirators adjourned while a messenger was sent to obtain
Mary's signature to the " bond of security." The queen,
before complying with the request, escaped to Dunbar,
and on her return to Edinburgh with an escort of 2000
men Morton and the other leaders fled to England. After
her marriage with Bothwell, Morton returned, and with
600 men appeared before Borthwick Castle, where the
queen, in dread of a rising, had taken refuge. He was
present at the remarkable conference at Carberry Hill,
and he also took an active part in obtaining the consent
of the queen at Lochleven to an abdication. Thereupon
he was reappointed lord high chancellor, and also succeeded
Bothwell as lord high admiral. On the death of the earl
of Mar he became regent (October 1572). Through his
persistence in recovering the crown jewels from the countess
of Argyll, widow of the earl of Moray, Morton awakened
the bitter animosity of Argyll and Athole, who persuaded
the young king James VI. to assume the government.
Morton deemed it prudent to resign, and for a time retired
to Lochleven, but shortly afterwards, with the assistance
of his nephew, the earl of Mar, he obtained possession of
Stirling Castle, where the king was residing, and thus for
a time recovered his old influence. Suddenly, however,
he was accused by James Stewart, earl of Arran, of having
taken part in the murder of Damley, the father of the
king, and being tried by a jury of sixteen peers, mosrt of
whom were his enemies, was condemned to death ^nd .be-
headed on 2d Jime 1581.
MORVEAU. See Guyton ds Morvead.
MOSAIC (late Greek ^Jiji^cxris, from >/^4">^, a small
stone ; also fiova-etov, i.e., refined, delicate work ; hence the
Latin opua musivum) is the fitting together of many,
generally small, pieces of marble, opaque glass, coloured
clays, or other substances, so as to form a pattern : the
XVL — 107
850
MOSAIC
dosign may bo of various degi'ces of elaboratiQii, from the
simplest, almost monochroniatic, geometrical pattern to
the rcost elalici-ate picture, with figiure-subjects represented
in colouis of countless gradations.
The earliest existing specimens of mosaic belong to one
of the less important branches of the art — namely, the
ornamentation on a small scale of jewellery, ivory thrones,
and other furniture, or more rarely of some elaborate archi-
tectural ornament. Most of thi.s earliest Eorfc of mosaic
resembles in exci":ution what arc called cloisonn'ee enamels.
In the Louvre and in the British JIuseura are preserved
some very beautiful ivory carvings in low relief, some from
Nineveh and others from Egypt, iu which figures of deities,
ornaments formed of the lotus and papjTUS plants, and
royal cartouches are enriched by small pieces of glass or
lapis-lazuli and other gem-liko stones, which arc let into
holes made in the ivory. Each minute piece is separated
from the next by a thin wall or clohon of ivory, about as
thick as cardboard, which thus forms a white outline, and
.sets off the brilliance of the coloured stones. The favourite
pattern in this sort of work for decorating the larger sur-
faces appears to have been suggested by the feathers on a
bu-d's v.-ing. See Ivoky, vol. siii. pi. vii. fig. 3.
Recent exeavatioriS at Tel al-YAhudfya in Lower Egypt
have brought to b'ght some mosaics on a larger scale, but
treated in the same way. These are caps of columns, wall
tiles, and other objects, either of white limestone or earthen-
ware, ia which designs, chiefly some forms of the papyrus,
Ero formed by brilliantly-coloured bits of glass or enamelled
earthenware, let into a sinking in the tUe or column.
This form of mosaic was employed by the Greeks : the
Erechiieom at Athens, built in the middle of the 5th
century e.g., had tho bases of some of its white marble
columns ornamented with a plait -like design, in which-
pieces of coloured glass were inserted to emphasize the
main lines of the pattern.
Another, quite different soi't of mosaic was known to
tho Egj'ptians of the Ptolemaic and Eoman periods. This
is made entirely of glass, ar-d is extremely miniite. The
finest known specimen is in tho Britisii I'useum : it is a
small tablet about three-eighths of an inch square, apparently
tho bezel of a ring, on which is represc.ited the sacred
liawk,^-cvery feather on the bird's wing being produced
with a great number of colours and tints, each quitj dis-
tinct, and so minute that a strong magnifying glass is
■ required to distinguish its details.
The way in which this wonderful little mosaic wiis pro-
duced is extremely ingenious. Numbers of long sticks of
various-coloured glass Y,-ere arranged in such a way that
their ends produced tho figuis of the hav.'k ; other sticks
of blue glass were placed aU round so as to form the
ground. The whole bundle of sticks of glass when looked
at endwise now presented tho figure of the hawk with a
blue backgroimd, immensely larger than it afterwards be-
came. The bundlo was then heated tiU the sticks melted
together, and tho wholo thick rod, softened by fire, was
then drawn out to a greatly-diminished thickness. In
this process the relative positions of the sticks of coloured
glass forming tho design were not altered. A slice of the
rod was thzn cut ofl', and its faces polished, — tho design,
much reduced in size, of course being equally visible at
both sides of tho slice ; and thus the microscopic minute-
ness of the mosaic was produced, with astonishing delicacy
and refinement ; many slices, each showing the same
mosaic, could bo cut from tho same rod.
The more important use of mosaic has been on a large
scale either for pavements or for walla and vaulted ceil-
ingu. Mosaic for these purposes has by many writei-s, both
ancient and modem, been divided on various systems into
<!.'',2M3a; periiapsthe simplest classification is thefollowing: —
I. For PavemontiA — (a) TesselcJed, in which the de£'.;::i
is formed of small cubes, generally of marble, more rarely
of glass or clay; (u) Scciile, formed of larger pieces of
marble, shaped and cut so as to fit accurately one with
another. II. For Walls and Vaults: — Fictile or vermicii-
laifd ; pieces o! opaque glass, in email cubes, arranged so
as to form complicated pictures.
This classification is not altogether satisfactory, more
than one method often behig employed in the same mosaic;
as, e.g., in the " opus Alexandrinura " of mediaeval writers,
which is often partly tesselated and partly sectilo.
Until Koman times we knov,- but little of these kinds of
mosaic. There is some evidence (in Pliny and other
writers) to show that elaborate mosaic pavements, Xi66-
(rrptDTov or Xi$o\i-p)iJjx, were m.ade by tho Greeks in the
4th century B.C., or even earlier ; but most or the nu-
merous fine specimens of tesselated work still existing in
Greece, such as these at Sparta and Athens, must be re-
ferred to the lime of the Roman occupation. Tlie best
e:3:ample3 of Hellenic mosaic are some pavements dis-
coTijred during, the recent excavations at Olympia (see
fig. 1 and Ansgrahingen sk O/ym^ta,' 1877-82).
Among the Romans the use of mosaic, both of marble
and opaque glass, was very extensive. According to
Pliny {H.N'., sxxvi. 25), they derived this art from the
Greeks, but not until the time o? the Tliird Punic War, HG
B.C., while glass mosaics for waUri, "vitreaj' parietcs,"
were a recent invention in his time. Many of these have
been foimd at Pompeii; most commonly they are used to
decorate niches for fountains or statuettes. Judging from
the description given by Vitruvius (vii. 1 ), and an examina-
tion of numerous specimens of Roman tesselated mosaics,
F;o. 1.— Grook Pavement from tl'.c Tci^ipio of Zeis i.t Olyraiii
the process of manufacture was the following. The earth
was first carefully rammed down to a firm and even surface ;
on this was laid a thick bed of stones, dry rubbish, and lime^
called "rudus," from 6 to 9 inches deep, au<l above this
another layer, 4 to 6 inches thick, called " nucleus," of one
part of lime to three of poundetl brick, mixed with water ;
on this, while still soft, the pattern could bo sketched out
mth a wooden or metal point, and the tes-serx or small bits
of marble stuck into it, with their smoothest side upper-
most. Lime, pounded while marble, and water were then
mixed to tho consistency of cream, forming a very hard-
setting cement, called " marmoratum." This cement, while
fiuid, was poured over the marble siu'face, and well brushed
into all the interstices between the tssserse. When the
MOSAIC
«51
concrete anJ cement were both set, the surface of the pave-
ment ■nas ruhVed down and polished. This kind of mosaic
wa3 largely used for floors of hypocausts ; the concrete bed
was then supported on large tiles resting on numbers of
short pillars.
If used for upper floors very strong joists were re-
quired, and both Pliny (xsxvi. 25) and Vitraviua (vii. 1)
recommend a double layer of boards, one crossing the other,
on which the concrete and cement bedding was to bo laid.
The usual Koman pavement was made of pieces of
marble, averaging from a half to a quarter of an inch square,
but rather irregular in shape. A few other, but quite
exceptional, kinds of mosaic pavements have been found,
such as that at the Isok Farnese, 9 miles from Eome,
made of tile-like slabs of green glass, and a fine " sectile "
pavement on the Palatine Hill, made of various-shaped
pieces of glass, in black, white, and dfeep yellow. In some
cases — e.ff., in the " House of the F^un " at Pompeii — glass
tesserse in small quantities have been mbced with the
marble ones, for the sake of greater brilliance of colour.
Pompeii is especially rich in its mosaics both on floor and
walls, almost every house having at least its vestibule
paved in this way.
In addition to graceful floiring patterns and geomctricul de-
signs, picture-like subjects of gi-eat elaboration frecpently occur:
of these the most important is the larOT and minutelj'-cxccuted
eceneofthebattleoflssus, found in the "House of the Faun." Itia
of special value as being the chief classical historical pictui-e still
existing. It is a well-desi.r^ed though somewhat crowded com-
p jsition, representing the moment of Alexander's victDi-ious charge
.-.c;ainst the cavalry of Daiius. The expression of the faces and
t!;e chttTacteriStic dresses of the Greeks and Persians are repre-
sented with great skill (see fig. 2). The tesserce, aa was always
tho case in this sort of work, are not all the same size, the smallest
(only about one-t»;nth of an inch squai-c) being reserved for the faces,
wV.ere greatest rciinemcnt of detail was required. This was a floor-
iMiiaic, thouch generally these rainutelyexecuted works were
itff'Xed to wells.
The most skilfully-executed of all existing mosaics of this pictorial
kind is that knox^ni as ** Pliny's Doves," found in Hadrian's villa
at Tivoli, and now ia the Canitoiine Museum. It may possibly be
the one so highly praised by Pliny (xxxvi. 25) as the work of Sosus,
for, although ho describes it as being at Pergamum, yet it was a
commou practice mth the Eom.in3 to transport these mosaics from
one place to another, and this verj' celebrated one m.iy well have
been brought to Tivoli to adorn the emperor's villa. It is treated
in a vei-y realistic way : the light on the gold bowl, the pluma"e of
the doves, and especially the reflexion in the water of the drinking
dove, are represented with wonderful skill. It is, in fact, far too
pictoi-ial, and, like the late mosaics in St Peter's, Rome, is more
remarkable for its technical skill than for any real artistic merit.
This exeessive realism, produced mth great difhculty and cost, is
a not uncommon fault of the more elaborate Roman mosaics, and
was the inevitable result of the luxury and ostentation of imperial
Home, which made art the bond-slave of the wealthy, rather than
tile free and natiu-al expression of a whole people, as it was among
the earlier Greeks.
Another interesting mosaic from the wall of a house at Pompeii,
of e.ttremely delicate work, is a rehearsal scene in a Greek theatre,
where the choregiis is instructing* the actors : it is specially re-
niarkable from its being signed as the work of Dioscoridcs of
Samos. Other tigiu-e-subjects are not uncommon, such as various
representations of the victory of Theseus over the Minotam-, others
of Achilles in Scyros, many hunting scenes, and the like.
Throughout England, Germany, France, Spain, Asia
Minor, and Northern Africa in no way have signs of
Boman occupation been left so clearly and in so con-
spicuous a form as by the numerous large and generally
well-preserved mosaic pavements which have at various
times been discovered in all these countries. In many
cases, long after all traces of the walls of the buildings
have disappeared, owing to their being dug up and re-
moved for building purposes, the mosaics still remain to
tdstify of the artistic power and mechanical skill of the
Bonian colonists.
Few countries are richer than England in these remains ;
the great pavements of York, Woodchester, Cirencester,
and many other places are as elaborate in design and as
skilfully executed as any that now exist even in Rome
itself. In whatever country these mosaics are found,
their style and method of treatment are always much the
same; the materials only of which the tesserse are mad^
vary according to the stone or marble supplied by each
country. In England, for instance, limestone or chalk
often takes the place of the white marble so common in
Italian and North African mosaics ; while, instead of red
marble, a fine sort of burnt clay or red sandstone is gene-
rally used ; other makeshifts had to be resorted to, and
many of the Anglo-Pioman mosaics are made entirely with-
out marble. It is perhaps partly owing to the great
wealth of Northern Africa in marbles of many colours and
of varying shades that the finest of all Eoman mosaics
have been found in Algeria and Tunis, especially those
'3 Hcia from tlic Battle of Issni ; ftiU blse.
from Carthage, some of which have been brought to the
British Museum. See Archosoloffin, vol. xxxviii. p. 202.
The range of colotir in the marble tesserre is very great,
and is made use of with wonderful taste and «kill : there
are three or fotir difl"erent shades of red, and an eijual
number of yellows and greens, the last colour in all its
tints being almost peculiar to this jjart of Africa, and one
of the most pleasant and harmoniou.s in almost any com-
bination. Deep black, browns, and bluisli-^'reys are also
abundant. The white marble which forms the grotmd of
nearly aU the designs-^s often not pure white, but slightly
striated with grey, giving great solLiiess and buiuty of
texture to the surface, and doing away with too great
monotony of tone. The Boman practice, common to all
their mosaics, of not fitting the tessene quite closely
together, but allowing the cement joints to show freoly,
was also of gieat value in giving effect to the general
texture of the surface — a jioiut quite forgotten by some
later mosaic-workers, who thought that the closer their
tessene were fitted together the better the mosaic would
be. This remark does not apply to sectile mosaic, in which
sufficient variety can be given by the markings and veins
in each piece of marble. To return to the mosaics from
Carthage, they are no less excellent in design than in
the richness and beauty of their materials. Large spaces
852
MOSAIC
are filled by grand sweeping curces of acantKus and other
leaves, drawn with wonderful boldness and freedom of
hand, and varied with great wealth of invention. With-
out the use of very small tesserae, much richness of effect
is given by gradations of tints, suggesting light and
shade, without a painful attempt to represent actual relief.
The colours of the marbles used here and elsewhere by the
Komans are so quiet and harmonious that it would have
]bcen almost imposbible to produce \vith them a harsh or
'glarii:;; design, and when used with the skill and strong
artistic feeling of the mosaic-workers at Carthage the
re^alt is a real masterpiece of decorative design. In
Kome, and in the Koman colonies of Europe, this kind of
marble tesselated mosaic was largely produced, with but
Jittle alteration in style or method of treatment, till the
4th century. In Syria and Asia Minor the art survived
some centuries later.
rcrliaps tlic lutcbt cxistin*; example in Rome 13 that which deco-
rates the vault of the ambulatory of the circular church of S.
'CosMiiza. built bv Conitautiue the Great (320), outside the walls
of Rome. Thi." very interestiDg mosaic might from its style and
materials have beeu executed in the 1st centiuy, and is equal in
beauty to any work of the kind in Italy. It shows no trace what-
ever of the Byzantine influence which, iu the next century, intro-
duced into Italy a novel style of mosaic, in materials of the most
glilteiing splendour. These S. Costanza mosaics are almost unique
in Italy as an application of the old classical marble mosaic to the
decoration of a Cbiistiaji church. On the main compartment of the
vault the surface is covered by vine branches, laden with grapes,
twining in graceful cur\ es over the space. In the centre is a large
medallion with life-sized male bust, and at the lower part are vintage
scenes — oxen carts bringing the grapes, and boys treading them in
a vat. Other more gcometiical designs, of circles fi'aming busts and
full-length figures, with giaceful borders, cover other parts of the
vault. Farther east this classical style of mosaic appears to have
lasted till the 6tli century. At Kabr-Hiraiu, near Tyre, JI. Renan
discovered among the ruins of a small thi-ee-apsed Christian church
a fine mosaic pavement, coveting the nave and aisles, thoroughly
classical in style. The design, consi^ing of circles enclosing figures
emblematic of the seasons, the months, and the winds, is almost
the same as that of some mosaics discovered on the site of the Roman
Italica near Seville, and othei-s at Ephesus and Halicarnassus in
Asia Jlinor. No trace of other than classical influence is visible,
and yet it is pretty clear, from the evidence of an inscription, inlaid
among the marble tesserre, that the date of this pavement is not
earlier than the latter part of the 6th century. A very similar
mosaic, of about the same date, was discovered at Neby Yunas, near
£idan.
Medistval Mosaics. — These may be divided into four
principal classes: — (1) those used to decorate walls and
.vaults, made of glass cubes ; (2) those for pavements, made
of marble, partly in large shaped pieces, and partly in small
tesserae ; (3) glass in small pieces, either rectangular or
triangular, used to enrich marble pulpits, columns, and
other architectural featiu-es ; (4) wood mosaics.
1 . The wall mosaics were, in their origin, purely Byzan-
tine, and appear to date from the beginning of the 5th
century. They are made of coloured glass, rendered opa'^ue
by the addition of oxide of tin. The melted glass was cast
into flat slabs, generally about half an inch thick, and then
broken into small cubes. Every possible colour and grada-
tion of tint was produced by the mediaeval glassmakers.
Tessera; of gold (which were very largely used) and^of
-silver were made thus : — the metal leaf was spread over
one of the glass slabs, the colour of which did not matter,
its it was hidden by the gold or silver ; over this metal-
coated slab a skin of colourless glass was fused, so as to
protect the metal leaf from injiu-y or tarnish ; and then
the slab was broken up into cubes, the }f^<f^i x/)vo-€oi of
iiiyzantine writers.
The method of putting together the mosaic w«s much
the same es that employed by the Romans in their tesse-
lated pavements. A thick coat of cement was applied to
thb wall or vault, the outline indicated witli a r.-.etal jwint,
nod the cubc-i stuck ono by one into the cement while it
was yet soft, — the main diiTerence being that no rubbing
down and polishing were required, the faces of the glass
tesserae showing the natural surface of the fracture, which
was not quite level, and by this slight ineqtiality of surface
great additional lustre and briUiauco of clTcct were given
to the whole picture.
Owing to the intense conservatism of Byzantine art, no-
regular stages of progression can be traced iu this class of
mosaic. Some of the 5th century mosaics at Ravenna are,
in every way, as fine as those of the 12th, and it was not
till the end of the 13th century that any important change
in style took place, when Cimabuo, and more especially
his pupils Jacopo da Turrita and Taddeo Gaddi, applied
their increased knowledge of the human form and of the
harmonies of colour to the production of the most beau-
tiful of all mosaics, such as those in the apse of S. JIaria
JIaggiore in Rome. -It must not, however, be supposed that
during all this time (from the 5th to the lith century)
one steady level of excellence was kept up. The mosaics
of the 9th century are inferior in drawing and general
treatment to those both of the earlier and later time, while
in Italy at least this art was almost entirely extinct during
the 10th and 1 1th centuries. Extreme splendour of colour,
and jewel-like brilliance combined with the most stately
grandeur of form are the main characteristic of this sort of
decoration. Its most frequent application is to the sanc-
tuary arch and apse of the early basilicas.
A "majesty," or colossal central figiiro of Christ with saints
standing on each side, is the most frequent motive. In many
cases, especially in the 5th and 6th centuries, Christ was represented
as a lamb, to whom the twelve apostles, in the fomi of sheep, aro
pajing adoration. Christ, the Good Shepherd, is sometimes depicted
as a beardless youth, seated among a circle of sheep — the treatment
of the motive being obviously taken from pa,gan representations
of Orpheus playing to the beasts. The tomb of Galla Placidia ii.as
a good example of this subject, with much of the old Roman grace
in the drawing and composition. Frequently the Virgin Mary, or
the patron saint of the church, occupies the centi'al space in the
apse, with ranges of other saints on each side.
The " Doom," or Last Judgment, is a favourite subject for domes
and sanctuary arches ; the Florence baptistery has one of the grandest
mosaic pictm'cs of this subject, executed in tlie 13th century. Tho
earlier buptisteries usually have the scene of Clirist's baptism, — tho
river Jordan being sometimes personified in a very classical mannei^'
as an old man with flowing beard, holding an urn from wiiich s
stream pours fonh. S. Vitale at Ravenna has in tho sanctuary a
very interesting representation of Justinian and his cmpre.ss Theo-
dora (see fig. 3), attended by a numerous suite of courtiers and
ladies ; these mosaics are certainly of tho 6th century, and may
be contemporary with Justinian, though the fact that ho onJ
Theodora are each represented with a circular nimbus appears to
indicate that they were not then alive. Scenes fiom both Old :>nd
Ne'.'' Testaments or the lives of tho saints arc also represented in
almost endless variety, — generally on the walls of the body of tho
church, in square-shaped pictures, arranged iu cue or luoro tici*s
over the nave cohmins or arcade.
In mosaics of the best periods the treatment of the forms
and draperies is broad and simjile, a just amount of relief
being expressed by delicate gradations of tints. In mosaics
of the Sth century the drawing is very awkward, and the
folds of the robes are rudely exjiressed iu outline, with no
suggestion of light and shade.
A further application of this work was to the decoration'
of broad bands over- the columns of the nave, as at S.
Mario ' Maggiore in Rome, 5th century, and in the two
churches of S. ApoUinare At Ravenna, Gth century. In
some cases almost the whole interior of tlie church wa.s
encrusted in this maguificeut way, as at Monrcale Cathedral,
the Capella Palatina of Palermo, and S. Mark's at Venice,
the magnificence of which no words can describe ; it is
quite unrivalled by that of any other buildings in the
world. See Monee,vle.
In these churches the mosaics cover soffits and angles
entirely, and give the effect of a mass of solid gold and
colour producing the utmost conceivable .^endour o£
MOSAIC
dLcoration? In many cases vaulteJ ceilings were coverei}
with these mosaics, as the tomb of Galla Placidia, 450
A.D., and the two baiJtisteries at Ravenna, 5th and 6th
centuries. For exteriors, the large use of mosaic was
usually confined to tlie west facade, as at S. Miniato,
Florence, S. Maria Maggicre, Home, and S. Mark's,
Venice. In almost ?,'" cases the figures are represented on
a gold ground, and gold is freely used in the dresses and
ornaments — rich jewels and embroidery being represented
in gold, silver, sparkling reds, blues, and other colours, so
as to give the utmost splendour of effect to the figures and
their drapery.
The revival of the art of painting in Italy and the
853
antroduction of fresco work in the Uth century gave the
deatliblow to the true art of waU-mosaic3. Though at
first the Bimple and archaic style of Cimabue and his
chnrJ^^^'^rfTi'^T **"' Wld-wide fame Of 3. Mark's and the other great
chnrches of Italy has subjected these extraordinary work, to the fatal
ClZli^ ^toration. " and wherever any sign of decay iu the cement
W «il /r-'' ^'^^^^'^ rt« "^'-^ auite indestructible) has given the
Zlb ^"^/"PP''«J»t» place with worthless modern copies. The
TvT: ^nH ?' ^* ^r^\ Wtislery. and of the apses at S. Miniato.
^'L\^'::iii:'^^^^ ^^^^ ^ ^^^^^ -^ ^- --^-^y -"--^
pupilfl Jacopo da Turrita, Giotto, and Taddeo GodA
was equally appHcable to painting or mosaic, yet soon the
development of art into greater realism and complexitj
required a method of expression unfettered by the necessi
ties and canons of mosaic-work. Pietro Cavallini, a Romar
artist, was one of the last who worked according to the
old traditions His mosaic of the birth of the Virgin in
; .u "*i l\ *^°'°^^^°» ^ome, executed about the middle
of the 14th century, i3 not ^-ithout merit, though hia
superior knowledge of form has only caused his composi.
wnrv! .f ^^'°'''^^^ ^^'^*' ^^^ '""''^''^ compared with the
works of the earher artists. Even in the 15th century a
few good mosaics were produced at Venice and elsewhere
binco then many large pictures have been copied in class
mosaic, generally attempts to imitate oil paintings, executed
with great skill and wonderful patience, but aU utterly
worthless as works of art, merely costly monuments of
human folly and misapplied labour. The mosaics from
Titian's pictures on the west end of S. Mark's at Venice,
Raphael's m the Chigi Chapel in S. Maria del Popolo, and
many large pictures in S. Peter's in Rome, are the moat
striking examples of these.
The following list, in chronological order, comprises a Bclectio*
from among the most important medieval glass wall-mosaics duriajr
tne penod when mosaic-working was a real art :—
5(/( Century.
Savenrui. Orthodox Baptistery— vault.
Tomb of Galla Placi-lia— vault, 450.
Archbiahop's Chapel— vault.
Boms, 8. Paolo fuori le mura— triurapbal arcb.
5. Maria Mas^iore— square pictures over oaTS colomuL aai
triumphal arch. — — »
ifilaiu S. Anibj-ogio, Chapel of S. Satiro— vault.
Fundi. Catliedr;:! apse.
Nola. Cathedral— apse.
6th Century.
Jiavenna. Arian Baptistery— vault.
6. Apolhnare Nuovo — apso and nave, with 9tk cftttary
Additions.
S. Vitale— apse and whole aanctuary, c(rca 547.
8. ApoUinare in Olasae— apse and nave, 649.
JtoTnt. 83. Cosmas and Damian— *p3e.
Milan. S. Lorenzo, Chapel of 3. Aquilinus— vault
Constantinople. S. Sophia— walls and vault, circa 550.
TIi€ssaloni«i. Church of &t George— ap^e, dec. ; and S. SophU— dMM tt4
TrOdsond. D. Sophia— apse.
7th Centxtrj/.
Home. 8. Af^iese ftaori le mora— apse, 626.
Jtrtualim.
8. Teodoro.
"Dome of the Rock" — arches of ambulatory, flW.
8(ft Centitrif.
Baptistpry of S. Giovanni in Latenmo.
m. Nereus and Achillee.
Mosque of AJ-Alcsa— on dome.
Chapel of the Transfiguration.
9th Century.
8. Cecilia In Trastevere— apse
8- MarcO'
8. Maria della Navicella— apsi
S. Prassede— triumphal arcn.
Conlova.
I, and "Chapel of Uc
ae— mumDnaj arcn.
8. Puden,
8. Ambrogio— apse, 832.
lOth CitUvry.
ilUirab (sanctuary) of Mosque.
nth Century.
" Dome of the Rock "—base of cupola, 1027.
JerusaUm ^ ^_
CoMtantinopte. Cboich af 8. 8a vioui^— walla and d'omeiT
_ Uth Century.
8. Mark i— uarthex, apse, and walU of nt\'e and alaloa.
Mun
Monreah.
Bethlehem.
Cefalu.
Bomt.
CathedrO— ajis
Cathedr VI — apse.
Cathedral— apse.
Cathedj »1— apse.
Capella Palatina, begun 1132— the whole iraila.
Church )f La Martorana — vault.
Cathcdf \1— the whole walla. 1170-00.
Church jftheXativity, 1169.
CathedJ-U- apse, 11 J&.
S. Cleif^nte— apse.
8. FrsDccsca Romnna — apse.
S. Uarj i in Trastev ere— Apse.
Ulh Century.
Baptif -tery vault, begun c. 1255 by Pro Jacopo.
8. Mt liato — apse and west front.
S. Po( 'lo fuori le mum— apse,
S. Cle 'ncnt*— triumphal arch, 1297.
8. Giavanni In taUrano — apse by Jacopo da Turrit^ L2M.
MagKiore— apue and we«t end by Jacopo A Ikirrfi^
854:
MOSAIC
UthCen^trf/.
^rmr>s»» Baptistery, finished by Andrea Tafl.
i .«r. CLthetlral— east apse by Cimabuo, 1302, north and south apses
by hi3 pupils.
y.jms, B. Iretcr's— na\1colla. In atriam by Giotto.
B. Mori.^ iu Cosmediu — oa w&Us by Pietro Cavalllni, e, 1340.
Venice. SS, Giovanai c Paolo— In nrcli over efBgy of Doge Morosini.
TLifl Ust 13 by no means ezdiaustivc, end only gives some of the
"best and inost typical examples of the mosaic-work of each century.
The Byzantine origin of these great wall-mosaics, wherever
they are found, is amply proved both by internal and documentary
cridence. The gorgeous mosaics of S. Sophia and S. Saviour's in
Constantinople, 6th century, aud the later ones in the monasteries
of Jloant Athos, at Salonica and at Daphne near Atiitns, are identical
in st)'lo with those of Italy of the same date. Moreover, the even
more beautiful mosaic-work in the "Dome of the Hock" at Jerusa-
lem, 7th and 11th centuries, and that in the sanctuary of the great
mosque of Cordova, of the 10th century, are knoi^-n to be the work
of Byzantine artist,^;, in snite of their thoroughly Oriental design.
The same is the case with the rarer mosaics of Germany, such as
those in S. Gereon at Cologne and at Parenzo.
A very remarkable, almost unique, specimen of Byzantine mosaic
is now preserved in the "Opera del Duomo," Floience. This is a
diptych of the 11th century, of extremely minute, almost micro-
scopic, work, in tessera; of glass and metal, perhaps the only example
of tesserse made of solid metal. It has figures of saints and inscrip-
tions, each tessera being scarcely larger than a pin's head. This
beautiful diptych originally belonged to the imperial chapel in Con-
stantinople, and was brought to Florence in the 14th century.
2. The second mediaeval class, mosaic pa\ cmcnta, though of great
beauty, are of less artistic importance.
This so-called " opus Alexandrinum " is very common throughout
Italy and in the East, and came to greatest perfection in tlie 13th
century. It is made partly of small marble tesscrie forming the
main lines of the pattern, and partly of large pieces used as a ground
or matrix. It is generally designed in large flowing bands which
interlace and enclose circles, often of one stone sliced from a column.
The finest exampleis that at S. Mark's, Venice, of the 12th century.
The materials are utaiidy white marble, with green and red poi"ph}Ty,
and sometimes glass.
Besides the coxmtless chnrches in Italy possessing these beautiful
pavements, such as S. Lorenzo, S. Slarco, S. Maria Maggiore, and
S. Marki in Trastevere, in Rome, we have, in the Chapel of the
Confessor, and in front of the higli altar at "Westminster, very fine
specimens of this work, executed about 1263 by a Roman artist
called Odericus, who was brought to England by Abbot Ware, on
the occasion of a visit made by the latter to Rome. Another
English example is tlie mosaic jtavemont in front of the shrine of
Becket at Canterbury; tliis is j.robably the work of an English-
man, though the materials arc foreign, as it is partly inlaid with
bronze, a peculiarity never found in Italy. There are also many
fine examples of these pavements iu the chiirchcs of the East, such
as that in S. Sophia at Trcbizond, of tlie most elaborate desic;n and
splendid materials, very like the S. JIark's pavement at Venice.
Palermo and Monreale are especially rich in examples of sectilo
mosaic, used both for pavements and walla, — in tlie latter case
generally for the lower part of the walls, the upper part being
covered with the glass mosaics. The designs of these Sicilian
works, mostly executed under the Norman kings in the 12th cen-
tury, are very Oriental in character, and in many cases wercactually
fxecuted by Moslem workmen. Fig. 4 gives a specimen of this
Tia. 4.— :.IarUe Hlosaic at Monreale Cathedral.
piosaac from Monreale cathedral. Its chief characteristic is tho
absence of curved lines, so largely used in tho splendid opus Alex-
andrinum of Italy, arising from the fact that this class of Oriental
deeign was mainly used for tho delicate panelling in wood on .their
pulpi*3, doors, &c., — wood being a material qoite nnsoited for iho
production cf large curves.
3. Glass mosaic, used to ornament amboncs, pulpito, t ^mba,
bishops' thrones, baldacchini columns, architraves, and other n.;>iblfl
objects, is chiefly Italian. Tho designs, when it is used to enrich
flat surfaces, such es panels or architraves, are very similar to x"! cac
of the pavements last described. The white marble is used as a
matrix, in which sinkings are made to hold the glass tesserce ; twisted
columns arc frequently ornamented with a spiral band of thia r^Iass
mosaic, or flutiogs are suggested by parallel hanth on sti.\'ight
columns. The cloisters of S. Giovanni in Latcrano and S. i':iolo
fuori le mura have splendid examples of these enriched EhaXts and
architraves.
This style of work was largely employed from the 6th to the l-icK
centuries. One family in Italy, the Cosmati, during the whole ol
the 13th century, was especially skilled in this craft, and the vaiioua
members of it produced an extraordinary amount of rich and beauti-
ful work. The pulpit in S Mai-xa in Ara Cor-h Rome is o*ie of the
finest specimens (see fig 5) as are aLo tl e ambones m S C'***
mente and S. Lorenzo,and
that in Salerno cathedral
The tomb of Henry III
1291, and the shrine ot
tho Confessor, 1269, at
V/estminster are the only
examples of this work
in England. They wer
executed by *' Pelntscivis
llomanns" probably a
pupil of tho Cosmati.
In India, especially
during the 17th conturj
many Mohammedan
buildings were decorated
with fine marble inlay of
the class now called ' ' Flor
cntinc." This is scclil
mosaic, formed by shaped
pieces of various-coloured
marbles let into a marblo
matrix. A great deal of
the Indian mosaic of th ^
.•^ortwas executed byltal
ian workmen ; the finest
examples are at Agra,such
as the Taj Mchal.
The modern so-caU^e I
*' Roman mosaic" is
formed of short and slen
der sticks of coloured glass
fixed in cement, the ends
which fonn the pattern
being finally rubbed down
and polished.
Many not unsuccessful
attempts have been mado
lately to reproduce the
Roman tcssclated work foi
pavements ; and at Mu
rano, near Venice, glass
^\ all -mosaics are still pro
duced in imitation of tho
niagnificL-nt works of me
di;LVal times.
4. Mosaics in wood are ^'o ^ -rare of m a
1 t T • Tif 1 mosa CI L.rc oiAi Cu. i
largely used m Moham
mcdan buildings, espcciallyfrom the 14th to thel/th centmies. The
finest specimens of this work are at Cairo and Damascus, and are used
chiefly to decorate the magnificent pulpits and other woodwork in the
mosques. The patterns are very delicate and complicated, worked
in inlay of small pieces of various-coloured woods, often further en-
riched by bits of mothcr-of-pcarl and minutely carved ivory. Tlio
general effect is extremely splendid from the combined beauties of
the materials and workman:)hip, as well as from the marvellous
grace and fancy of the designs. Tliis art was also practised largely
by tho Copts of Egypt, and much used by them to ornament tho
magnificent iconostascs and other licrcens in their churches.
Another a}>plication of wood to mosaic-work, called "intarsia-
tnro," was very common in Italy, c.snccially iu Tuscany and Lom-
bardy, during tho 15th and early 16th centuries. Its chief use was
for tlie decoration of the stalls and lecterns in the church-choira.
Very small bits of various-coloured woods were used to prodnca
geometrical patterns, while figui-c-subjects. views of buildings with
strong yicrspectivc elTccts. nnd oven landscapes, were very skilfully
produced by nn inlay of Inrger pieces. Anibrogio Borgognone,
Raphael, and other great painters often drew the designs for this
soit of work. The mos.iic figures Lu tha panels of the stalls at the
H O S-.M 0 S
855
Gertosa near Pavia were by Boigopioiie, .".nd are extremely bsauti-
foJ. Thd stalls in Siena cathedral and in S. Pietro d6' Casinensi
at Perugia, the latter from Rapiiael's designs, are among the firest
works of this cort, which are vciy numerous in Italy. It has also
been used on a smdlcr scale to ornament furniture, and especially
the ** Ca.9soni," OT largo trousseau coffers, on which the most costly
and elaborate decorations were often lavished. Some traditional
skill in this art still lingers in Italy, especially in the city of Siena.
AuTUoniriEa.—ClasstcaZ ^twato.— Pliny, ff. N., xxxvi. ; Vitniviua ; Franks,
Slade Collection of Ancient Glass, and Exavatlana at Carthage, 1860; Artaud,
Uislolre de la pelnture en mosaXque,. 1835 ; ifonumcntoi Arqttitfctonlcoe de Espana
("Italica," "Cordoba,"' and "Elcho"), 1859-83 ; Liilionle, Mosa:ique d'ltalica,
pres de Seville, 1802 ; Ciamptni, Veiera Monvvienta, Koine, 1747 ; A'on Minutoli,
ifosaikfussbodoi, &c., 1835 ; Lysona, Mosaics o/ UorkUow, 1801, and Jlomau
Antiquities of Woodchester, 1797 ; Mazda, Lea mines de Pompii, Paris, 1812-38 ;
RtaX Museo Borbonico, various dates; Ruach Sioith, Bcuian LondOTi^ 1859;
Ausgrabung'eit zii Olympia, 1877-82.
Christian.— Tiieo-philua, Diversarum Artium ScheduUu U. 15; S. Kenslnfjtoii
Miuieum Art Inventory, part 1., 1870 ; Itcniin, Mission de PlUnicie, 1875 ; Gamicci,
Arte Crisliana, 1872-82. vol. iv. ; De Uossf, Musalci Cristiani di Jioma, 1872-82 ;
Parker, jircAafo^offff of Rome, and Moxatc Pictures in Rome and Savcnna, 1866 ;
Jouy, L&3 MosaXques ehrHiennes tie Home, 1857 ; Qrevina, Duomo di Monreale,
Palermo, 1859 $q. ', Serradifalco, Monreala cd altrc ehiese Siculo-Normanne, 18C8 ;
Salazaro, Moit. delV ArUMerid. d'lUtlia^ 1882 ; M. D. Wyatt, Geometrieul Mosaics,
of tJte Middle Ages, 1849; Sa.lzQn'borg, A U-Christliche LaiuUnkntale von Constanti-
nopel, 1854; Pulgher, Eglises Byzantincg de Constantinople, 1888; Texicr and
Pullan, Byzantine Architecture^ 1864 ; Qiiast, Alt-ChrUsUicken Bauwerki von
Saveniia, 1842 ; De VogQft, Eglises de la Terre Salute, 1860; Milancsf, Del Arte
del VttTxt pel Mtaaico, 16th century (reprinted at Bologna in 1864) ; Rohault de
FUwryJ_Monuv^ents de Pise, 18CG; Krcutz, Basilica di S. Marco, P'euczin, 1813;
Gaily Knight, Ecclesiastical ArchltvetuTe of Italy, 1842-1 ; Foasati, Aya Sophia,
1852 ; Didron, " La peinture en Mosai'que," Cfaz. des B. Arts, voL :u., p. 412 ;
Gerspach, Iai Mosa'igue, 1883.
Jtfosltfm.— Hessemer, Arabische uvd Alt-ItalieniscJie Bau-Verstervnoen, 1853;
18*8 ; Coatc, Monuments modernes dt la Perx, 1867 ; Flandin and Co^tc, Voyage
tn Perse, 1843-64.
JFood- Mosaic— Tarsia.— Or natl del Coro di 3. Ptetro Casstnenso di Perugioy
MOSCHELES, Ionaz (1794-1870), one of tie most
refined and accomplished pianists of the present century,
was born at Prague, 30th May 1794, and first studied
music at the Conservatorium in that city under the direc-
tion of Dionys Weber. At the age of fourteen he made
his first appearance before the public in a pianoforte con-
certo of his own composition with marked success. Soon
after this he removed to Vienna, where he studied coun-
terpoint tinder Albrechtsberger and composition under
Salieri. In 1814 he prepared, with Beethoven's consent,
the pianoforte arrangement of Fidelia, afterwards published
by Messrs Artaria. In tho following year he published
his celebrated Variatioiun iihei- den Alexandermarsch, a con-
cert piece of great difficulty, which he j^layed with so great
eflect that he was at once recognized as tho most brilliant
performer of the day. Ho then started on a tour, during
the course of which ho visited most of tho great capitals
of Europe, making his first appearance in London in 1822,
and there securing the friendsliip of Muzio Clementi and
John Cramer, the fathers of the English school of piano-
forte playing. For a concert given by the latter he
wrote his famous Hommage d, Handel, a duet for two
pianofortes, which afterwards became a lasting favourite
with the pub'ic. His reception in England was sufficiently
encouraging to justify his retm-n in 1823, when ho again
met with a liunrty welcome. During a visit to Berlin in
18- i he first became acquainted with Mendelssohn, then
a boy of fifteen ; and a friendship .sprang up between them
which was severed only by Mendelssohn's early death.
In 1826 Moscheles relinquished his wandering habits,
aiid settled permanently in London, surrounding himself
%vith a clientele fully capable of appreciating his talents as
an artist and his social worth as a firm and loyal friend.
His position was henceforth a more than ordinarily en-
viable one. He was recognized from end to end of Europe
as a virtuoso of the highest rank ; and his popularity both
as a performer and as a teacher was based on grounds which
effectually secured it from the caprice of changing fashion or
ephemeral patronage. He was undoubtedly for some con-
siderable time the greatest executant of his age; but, using
his brilliant touch a,s a means and not as an end, he con-
eistenlly devoted himisolf to the further development of the
trufc 4assical school, interpreting the works of the great
masters with conscientious fidelity, and in hia extempore
performances, which were of quite exceptional excellence,
exhibiting a fertility of invention which never failed to
please tho most fastidious taste.
In 1837 Moscheles conducted Beethoven's Ninth Sym-
phony at the Philharmonic Society's concerts with extra-
ordinary success ; and on thla and other occasions contri-
buted not a little, by his skilful use of tho baton, to the
prosperity of tho time-honoured association. During the
course of his long residence in Loudon he laboured inces-
santly in the cause of art, pla)ring at innumerable concerts,
both public and private, and instructing a long line of
pupils, who flocked to him, in unbroken succession, until
the year 1848, when, at Mendelssohn's earnest solicitation,
he removed to Leipsic, to carry on a similar work at tha
Consei-vatorium then recently founded in that city. In
this new sphere he worked with unabated zeal for mora
than twenty years, dying 10th March 1870.
Moschelea's most important compositions aro liis Pianolbrte Con-
certos, Sonatas, and fatuilies; his Homviagc <k UHnddx and bCi
three celebrated Alter/ri di Bravura.
MOSCHUS, of Syracuse, is one of the Greek bucblio
poets ; he was a friend of the Alexandrian grammarian
Axistarchus (about 200 B.C.). His chief work is the epi-
taph of Bion of Smyrna, another of the bucolic poets,
who seems to have lived in Sicily. It is probable that tho
miscellaneous collection of poems which we possess by the
three poets Theocritus, Bion, and Moschus was known to
Artemidorus in 200 B.r. Hia poetry is the work of a well-
educated man with a tinned artistic eye ; he models hia
works on those of Bion, writing epigrammatic, epic, and
idyUic or elegiac verses, all except a few lines being in
hexameter verse ; but he treats all his subjects in a de-
scriptive, not in a narrative or an epig/ammatio stylo.
Besides the epitaph of Bion, he wTote two little epic poems,
"Europa" and "Megara," and a pretty little epigram,
" Love the Rtmaway ; " and a few short pieces of his are
also preserved. They are written with much elegance, but
the style is perhaps too refined and carefully wrought, and
he has few of the higher qualities of a poet.
MOSCOW, a government of Central Russia, bounaed
by Tver on the N.W., Vladimir and Ryazan on the E.,
Tula and Kaluga on the S., and Smolensk on the W., and
having an arer. of 12,858 square miles. The sm-face is
undulating, with broad depressions occupied by the rivers,
and varies in elevation from 500 to 850 feet. Moscow is
situated in the centre of the so-called Moscow coal-basin,
which extends into the neighbouring governments, and
consists of limestones 6f therUpper and Lower Carboni-
ferous, 'the latter containing beds of inferior coal, while
the former contains several good quarries of marble. The
Carboniferous foi-mation is covered with Jurassic clays,
sandstones, and sands, which yield a good china-clay at
Gjeli, copperas, a sandstone much employed for building,
and a white sand used for the manufacture of glass. The
whole is thickly covered with boulder-clayand alluvial sands.
The government is watered by tho Volga, which skirts it for a
few miles on its northern boundary, by the navigable Scstra, which
brings it in communication witli the canals leading to St Peters-
burg, by tha Oka, and by the Moskva. This lost takes its origin
in Smolensk, and, after a course of 230 miles right across Moscow,
reaches the Oka at Kolomna ; it is navigable from the town of
Moscow. The Oka and Moskva from a remote period have been
important channels of trade, and continue to bo so not^thst.mding
the development of railways. Tho Oka brings the government
into water commu.iication with the Volga, whoso tributaries cover
nearly the whole of middle and eastern Kussia, and arc separated
by short land distances from the Northern Dwlna and the Don.
Large quantities of grain, metals, glass ware, skins, and other com-
modities are shipped up and doivn tho Moskva, whilst the Myach-
kovo stone quarries situated on its banks supply the capital with
building stone. There are several marshes, mostly, in the north
856
M O S CJ O VV
where also, as well as in tlm nortL-cast, notwithstandiu^; tlic
inimtnsc consiimiitinn of wooil in inanufactuies and for use in tlio
capital, c-xtensive forests are still found. Very large supplies of
timber are al&o imported li}- rail or river, especially from the adjoin-
ing norili-easlgrn provinces. The soil is somewhat unproductive,
the average crops ranging from SJ to 43 returns; agriculture
is eavrictl on everywhere, but only two districts (Ruza and Yolsko-
lamsk) export corn, all the others being more or less dependent
on extraneous supplies. The agiicultural holdings of the peasants
arc very small, and their condition on the whole unsatislactory.*
Crass erojis have vome importance in sevci-al districts, and kitchen-
gardening is an important source of wealth in Vereya, Diuitroff,
and Zvenigorod. Cattle arc not extensively reared, but the horse-
breeding industry is somewhat important
The population, 1,581,700 in 1864, numbered 1,913,700 in 1873,
one-third being urban. They arc nearly all Great-Russians, and
belong to the Creek Church, or are nonconformists, ilany are
employed in factories, the number of which in 1879 was 1546,
occupying 162,700 hands, and having an annual production of
about £20,000,000 sterling. These figures show the manufactur-
iiig activity of ^Moscow to be greater than that of any other Russian
government, while the value produced is upwards of one-fifth of
the total for nil Russia in Europe, including Poland. Cotton,
woollen, and silk goods arc the chief products. The sanitary
condition of the factories is very bad ; the number of children
bflow fifteen years employed is as high as 16 per cent., the hours
of daily work are often 13 to 16, and the mortality is very great.
The total income obtained by the populationof the government from
their manufacturing industry is estimated at £485,600. The chief
income of the pcojjlc is derived, however, fi;om a variety of petty in-
dustries, carried on in their villages by the peasants, who continue
at the same time to cultivate the soil. Taxation during the last
twenty years has been increasing rapidly, and in some parts of the
government has reached an average of 12 roubles per house. The
chief centres of tjade are Moscow, Kolomna, Serpukhoff, Bogorodsk,
Scrghievsk, and Pavlovsk. Thcie are 125 fairs. Transport is much
facilitated by railways, and by good highroads radiating fi-om
the cajiital. Moscow is divided "into thirteen districts, the chief
town's with their respective populations being — Moscow (670,000),
Bogorodsk (C600), Bronnitsy (3500), Rnza (4000), Kolomna (18,800),
Serpukhoff (16,800), Podokk (11,0001, Zvenigorod (7800), Mojaisk
(4200),Volokolamsk (3000), Klin (6700), Dmitroff(7600),and Vereya
(5500). In addition to these administrative centres may he men-
tioned Voskresensk (6000), Serghievski Posad (27,500), in the
neighbourhood of the monastery of Troitsa, a rich commercial and
industrial town, and Pavlovski Posad (4500). Many of the villages
are far more important from their industries and trade than the
district towns.
MOSCOW (Russian, juostva), the second capital of
the Eussian empire and chief towTi of the government
and district of the same name, is situated in 55° 45' N.
lat. and 37° 37' E. long., on both banks of the river
Moskva, a tributary of the Oka, at its confluence with
the rivulet Yauza. The popular idea is that Moscow is
built on seven hills, and in fact the city covers several
eminences, tlie altitudes of its different parts varying from
500 to 850 feet above the level of the sea. It is 400
miles from St Petersburg, 813 from Archangel, 900 from
Ufa, 938 from Astraklian, 933 from Odessa, and 811 from
Warsaw. It lies to the north of the most densely-jjeopled
parts of Russia (the "black-earth region"), whilst the
country to the north of it is rather thinly peopled as far
as the Volga, and very sparsely beyond that. The space
between the middle Oka and the Volga, however, was the
very cradle of the Great-Russian nationality (Novgorod
and Pskov excluded) ; and four or five centuries ago Mos-
cow had a quite central position with regard to this.
The present city measures 7 miles from north to south,
and 9 miles from west-south-west to cast-north-east, and
covers an area of 32 square miles (about 40 when the
suburbs are included). In the centre, on the left bank of
the Moskva, stiinds the " Kreml " or Kremlin, occupying
the Borovifsky hill, which in the 12th century was covered
by a dense forest. ' To the east of the Kremlin is the
Kitay-Gorod, formerly the Great Posad, the chief centre
' According to recent investigations instituted by the Moscow pro-
\incial assembly, 10 per cent, of the agricultural poptdation (about
20,000 households) have no laud at oil ; 15 per cent., while holding
laud, are bankrupt ; and 13 per ceuu are without cattle or implemcuts.
for trade. The Byelyi-Gorod, which was formerly enclosed
by a stone wall (whence the name), surrounds the Kremlin
and the Kitay-Gorod on the west, north, and north-east.
A line of boulevards now occupies the place of its wall
(destroyed in the ISth century), and forms a first circle
of streets arnimd the centre of iloscow. The Zemlanoy-
Gorod (earthen enclosure) surrounds the Bj'elyi-Gorod,
including the " Zamoskvoryechie " on the right bank of
the Moskva. The earthen wall and palisade that formerly
enclosed it no longer exist, their place being taken by a
series of broad streets vdih gardens on both sides, — the
Sadovaya, or Gardens Street. The fourth enclosure (the
"Kamer-College earthen wall") was made during the reign
of Catherine II. ; it is of irregular shape, and encloses the
outer parts of JIoscow, whilst the suburbs and the villages
which have sprung up on the highways extend 4, 5, and 6
miles beyond. The general view obtained from the west
or south is very picturesque, especially on account of
the numerous churches, monasteries, and towers with
characteristic architecture, and the many gardens and
ponds scattered among clusters of houses. "The Kremlin
is an old fort of pentagonal (nearly triangular) shai)e, 98
acres in extent, occupying a hill about 100 feet above tha
level of the Moskva. It is enclosed by a high stone wall
2430 yards in length, restored during the present century,
and having eighteen towers. Its five gates are surmounted
by high towers. The Spasskiya (Saviour's Gate) was
erected in 1491 by a Milanese architect, the Gothic tower
that surmounts it having been added in 1626 by the
English architect HoUoway. A sacred picture of the
Saviour was placed upon it in 1GS5, and all who pass
through the gate must uncover. The towers surmount-
ing the four other gates were erected by order of Ivan
III. Of the sacred buildings of the Kremlin the most
venerated is the Uspensky cathedral. The former church
of this name was erected in 1326 by Ivan Kalita, but, on
its falling into disrepair, a new oiie was built on the same
place in 1475-1479, by Fioraventi, in the Lombardo-
Byzantine style, with Indian cupolas. It was restored
in the 18th century and in 1813. It contains the oldest
and most venerated holy pictures in Russia, one of which
is attributed to the metropolitan Peter, another to St
Luke. This last was brought from Kieff to Vladimir
in 1155, and thence to Moscow in 1395; its jewelled
metallic cover is valued at £20,000. The cathedral pos-
sesses also a gate brought from Korsun, the throne erf
Vladimir I., and numerous relics of saints, some of
which date from the 14 th century. The Russian metro-
politans and patriarchs were consecrated in this cathedral,
as well as the czars after Ivan IV. The Arkhangelsk
cathedral was originally built in 1333, and a new one was
erected in its place in 1505. It has suffered very much
from subsequent restorations and decorations. It contains
the tombs of the czars from Simeon (1353) to Ivan
Alexeevitch (1696), and possesses vast wealth. The Bla-
govyeschensk cathedral, recalling the churches of Athos,
was built in 1489; the remarkable pictures of Rubleff
(1405), contained in the original structure of 1397-1416,
have been preserved. It was the private chapel of the
czars. Vestiges of a very old church, that of the Saviour
in the Wood {Spas n<t bori7), contemporaneous with the
foundation of JIoscow, still exist in the yard of the palace.
A stone church took the place of the old wooden structure
in 1330, and was rebuilt in 1527, Several other churches
of the 15th century, with valuable archxological remains,
are found within the walls of the Kremlin. The Vozne-
scnsky convent, erected in 1393, and recently restored
with great judgment, is the burial-place of wives and
sisters of the czars. The Chudoff monastery, erected in
1365, was the seat of theological instruction and a stata
M o rs c o w
857
prison. Closa by, iLo gre:if campanile of Ivan Veliky,
erected in tho Lombardo-lJyzantiDe style by Boris Godunoff
in 1600, rises to the height of 271 feet (328 feet including
the cross), and contains many bells, one of vrhich weighs
1285 cwts. The view of Moscow from this campanile is
really wonderful, and its gilded cupola is seen from a great
distance. Close by is the well-known Tsar-Kolokol (Czar of
the Bells), 60 feet in circumference round the rim, 19 feet
high, and weighing 3850 cwts. It was cast in 1735, and
broken during the fire of 1737 before being himg. The
treasury of the patriarchs (riznitsa) contains not only such
articles of value as the sahhos of the metropolitan Foty with
70,000 pearls, but also very remarkable monuments of Rua-
<iian archeology. The library has 500 Greek and 1000
very rare Bossian MSS., including a Go9peI of the 8tli
century.
The great palace of the emperors, erected in 1849, is a
fine building in white stone with t. gilded cupola. It con-
tains the Urems, or rooms erected for the young princes ia
1636 (restored in 1836-1849, their former character being
maintained), a remarkable memorial of the domestic life of
the czars in the 17 th century. In the treasury of the czars,
Granovitaya Palata and Orujeynaya Palata, now public
museums, the richest stores connected with old Kussian
archseology are foimd — crowns, thrones, • dresses, various
articles of household furniture belonging to the czars,
Russian and Mongolian arms, carriages, ifec.
The four sides of the Senate Square aie occupied by
Plan of Moscow.
buildings of various dates, from the 15th century onwards.
The senate, now the law courts, was erected by Catherine
JI. Facing it is the arsenal, containing full ammunition
for 200,000 men.
The Temple of the Saviour, begun in 1817 on the
Vorobiovy hills, in commemoration of 1812, was abandoned
in 1827, and a new one was built during the years 1838-
^ 1881 on a hill on the bank of the Moskva, at a short dis-
tance from the Kremlin. Its style is Lombardo-Byzantine,
with modifications suggested by the military taste of
Nicholas I. Its colossal white walls are well proportioned,
and its gilded cupolas are seen from a great distance.
^e buildings that surround it are to be clestfed away,
fmi its wide squares adorned by obelisks, and by monu-
ments to Kutuzoff, Barclay de- Tolly, Alexanc.er L, and
Nicholas L
The Kitay-Gorod, which covers 121 acres, and has
20,000 inhabitants, is the chief commercial quarter of
Moscow. It «ontains the Gostinoy Dvor, coisisting of
several stone buildings divided into 1200 shop), where all
kinds of manufactured articles are sold. The "Red Square,"
900 yards long, whose stone tribunal was formerly tho
forum, and afterwards the place of execution, separates the
Gostinoy Dvor from the Kremlin. At its lower end stands
the fantastic Pokrovsky cathedral (usually kncwrfas Vasili
Blajennyi), which is the wonder of all stranger* visiting
Moscow, on account of its towers, all differing from each
other, and representing, in their variety of colours, pina-
XVT. — loS
858
MOSCOW
apples, melons, and the like. . It •was built under Ivan the
Terrible by an Italian. The exchange, built in 1838 and
restored in 1873, is very lively, and its tvrenty-three
"exchange artels" (associations of nearly' 2000 brokers,
possessing a capital of more than ^lOO^OOO) are -worthy of
remark. Banks, houses of great commercial firms, streets
full of old bookshops carrying on a very large trade, and
finally tho Tolkuchy rynok, the market of the poorest
dealers in old clothes, occupy the Kitay-Gorod, side by side
with restaurants of the highest class. In the KLitay-Gorod
are also situated the house of tho Romanoffs, rebuilt in
1859 in exact conformity with its former shape; a Greek
monaster)' ; and the printing-office of the synod, containing
about 600 MSS. and 10,000 very old printed books, to-
gether with a museum of old typographical implements.
At the entrance to the Kitay-Gorod stands the highly-
venerated chapel of the Virgin of Iberia, which is a copy,
made in 1648, of a holy picture placed on the chief gate
of the monastery of Athos. Close by is the recently opened
historical museum, which will contain collections respect-
ively illustrating separate periods of Russian history.
The northern parts of the Byelyi-Gorod are also the
centre of a lively trade. Here are situated the Okhotnyi
Ryad (poultry market) and the narrow streets Tvei-skaya
and Kuznetsky-Most, the rendezvous of the world of fashion.
Here also are the theatres. In the south-west of the Byelyi-
Gorod, opposite the garden of tho Kremlin, stand the uni-
versity, the public museum, and the military riding school.
The Zemlyanoy-Gorod, which has arisen from villages
that surrounded Moscow, exhibits a variety of characters.
In the neighbo\u-hood of the railway stations it is a busy
centre of traffic ; other parts of it are manufacturing
centres, whilst others — as, for instance, tho small quiet
streets in the west of the boulevard of Prechistenka, called
the old Konushennaya, with their wooden houses find
spacious yards — are the true abodes of the families of the
old, for the most part decayed, but still proud nobility.
The Zamoskvoryechie, on the right bank of the Moskva,
is the abode of the patriarchal merchant families. Each
house is surrounded by a yard whose gat« is rarely opened,
and each house, with its dependencies and gardens, bears
the character of a separate estate.
Tlie climate of Jtoscow is cold and continental, but heaUli|-.
The average annual temperature is 40°'l Fahr. (January, 14 ;
July, 6C°-o). The summer is warm (64°-2), and tho winter cold
.ind dry (IS^'S), cpeat masses of snow covering the streets. The
spring, as is usu^illy tho case in cold continental climates, is beauti-
ful. The prevailing winds are south-u-est and south. The river
Moskva is frozen, on the average, for 153 days (from 12th Novem-
ber to 13th April>.
Besides tho Jloskva and the Yauza, Moscow is watered also by
the NcUnnaya, vrhich now flows in an uudergi'ound channel under
the wafls of the Kremlin. The city has about 200 ponds. Tho
Moskva is crossed by five bridges ; a branch of it, or rather a
channel, makes an elongated island in the centre of the town.
Water of excellent quality, principally from the Mytischi springs
and ponds, 11 miles distant, is led to fouuteins in different parts
of the town, whence it is taken by watermen. But this supply
amounts only to 1,865,000 gallons a day, and the gi-eat mass of tho
inhabitants make use of the contaminated water of tho Moskva
and even of the Yauza, or of private wells.
Tho population of JIoscow, which is steadily increasing, is esti-
mated at 070,000 ; but an accurate census has not yet been made.
In the middle of the 18th century it was estimated at only 150,000 ;
in 1812, at 250,000 in summer and 400,000 in ivintor. In 1864 it
was estimated (probably under tho truth) at 305,000. The inhabit-
ants are mostly Great-Kussians, and only about COCO are foreigners.
They chiefly belong to the Greek Church, or are nonconformists,
the number of Lutherans and Catholics being only 8000 to 9000.
The mortality is very gicat : in 187a.and 1330 it reached 37-9 and
41-8 per thousand (men 39-3 ; wonfdn 43-9), and usually exceeds
the birth-rate. Moscow, moreover, is often visited by epidemics
■which immensely increase tho mortality, in consequence of the
almost entire absence of sanitary regulations. Fires are very fre-
quent; within tea years (1870-1879) thoy numbered 2492, the loss
being estimated at £2,865.300.
Since the 1 4th century Moscow has been an important comme^
cial city. Its merchants carried on a brisk trade with Novgorod
and Pskov, with Lithuania, Poland, Hungary, Constantinople^
Azofl', and Astrakhan. About the end of the loth century its
princes transported to Moscow, Vladimir, and other Russfau towns
no fewer than 18,000 of the richest Novgorod merchant families,
and took over the entire trade of that city, entering into direct
relations with Narva and Livonia. The shops of the Gostinoy
Dvors of Moscow astonished foreign visitors in the 16th century
by their large supply of foreign wares, and by the low prices at
which the products of western Europe were sold, — a circumstance
explained by the barter character of the trado. Tho annexation
of Kazan and the conquest of Siberia gave a new importance to
iloscow, bringing it into direct commercial relations with Khiva,
Bokhara, and China, and supydying it mth .Siberian fur9._ The
fur-trade engrossed the minds of all European merchants in the
16th century, and an English company, "The Mystery," having
received the monopoly of the Archangel trade, caused tho traffic
to be sent by the ^V^^ito Sea instead of the Baltic. Moscow thus
became tho centre for nearly the whole trade of Russia, and th»
czar himself engaged in largo commercial operations. All boyors,
and tho church too, were traders ; and the poorest Moscow per
chants participated in the trade through their corporations.
Persians, Greets, Armenians, Swedes, English, Germans, and
Lithuanians had each its own Gostinoy Dvor (or caravanserai).
Situated at the junction of six important highways (along which
communication was maintained by special yamshiks), Moscow was
the gi-eat storehouse and exchange-mart for the merchandise ot
Europe and Asia. The opening of the port at St Petersburg affected
its commercial interest unfavourably at first ; but the Asiatic and
internal trade of Moscow has since then enormously increased. At
present it is the chief centre of railway traffic. The revenue of its
custom-house was in 1880 double that of St Petersburg (30,000,000
roubles, as against 15,620,000 at St Petersburg and 9,000,000 at
Warsaw). ?3ut tho~home tTaflic is the most important branch of the
Tiloscow trade. Tho city is the chief centre for the trade in grain, in
hemp, and in oils, sent to tho Baltic ports,; in tea, brought both 1^
.Siberia and by St Petersburg ; in sugar, refined there in large quanti-
ties ; in grocery wares for the £ui>ply of more than half Russia and
all Siberia ; in tallow, skins, wool, metals, timber, wooden wares,
and all other produce of the manufactures of middle Rusiia. No
less than 10,000,000 cwts. of corn are annually brought to Moscow,
half of which is sent to the Baltic ports. Tho yearly return of tho
Moscow trade was estimated at £9,000,000 in 1848,— probably only
a half or a third of the real value, which is believed to have been
at least trebled since that rime. The quantity of goods carried by
the six railways from Moscow to St Petersburg, Yaroslav, Nijm,
Ryazan, Kursk, and Brest, amounted in 1878 to 162,343,500 cwta.
(out of 635,740,000 for tho whole of Russia) ; and the number of
pnsseugeis was 8,637,890 (1,263,530 military) out of a total for all
Kiissia°af 37,580,800 (civil and military) in that year.
From the 15th century onwards the villages around Moscow were
renowned for the variety of small trades they carried on ; the first
large manufactures in cottons, woollen fabrics, silk, china, and
glass in Great Russia appeared at Moscow in the 17th and ISth
centuries. After 1830, in consequence of protection tarifi's, the
manufactories in the government of Moscow rapidly increased in
number ; and at present two-thiids of them, or about 1000, annu-
ally producing articles to tho value of upwards of £10,000,000 (th»
real production is probably much higher), ara concentrated in th»
capital. There are at Jioscow about 170 cotton-mills, CO manu-
factories of woollens, and 79 of silks, the silk manufafiured being
chiefly Caucasian, although a good deal is also imported from tho
west ; there are also upwards of 20 large tanneries, 50 tobacco-
factories, 15 lar^ candle-works, 70 larger workshops in metals, 13
wax-candla works, 30 carriage manuiaotories, 20 watch manu-
factories.
The income and oxpenlituro of Moscow in 1682 were respectively
4,921,067 and 6,124,063 roubles, as compared with 4,730,724 and
5,490,433 in 1S81.
Moscow has many educational institutions and scientific societies.
The universitv, founded in 1755, exercised a powerful influence on
tho intellectual life of Russia during tho years 1S30-184S; and
it still continues to be the most frequented ftussian university. lu
1882 it had 2430 students .and a teaching stalf of 334 ; the studenta
are mostly poor, tho sum of 107,588 roubles having been given
in ISSl in scholarships to 854 of their number, and 14,000 roubles
in the form of occasional assistance. Tho librnry contains nearly
200,000 volumes, and has rich collections in mineralogy, geology,
and zoology. There is also an excellent higher technical school ;
and an ogiicultuial college is situated in the Petrovskoyo suburb,
filoscow has also a theological academy, a commercial academy, a
school of topography, an institute (of Lazareff) for the study of
Oriental languages, a musical conservatory, f)ur institutes for
women, a free university for vomer, seven colleges for boys and
three for girls, three corps of military cadets, very numerous
primary and leclwicAl schools^ *^ jaauy private schools, J*
MOSCOW
859
ittill tbeM u« /nsnfficient for the popnlation, and the. monicipal
fcohoola crery year refoso adznlBsion to about 1600 boys and girls.
Tho ecientific societies are specially distinguished for their services
in the oxplomtion of the country. Tho following deserve parti-
cular mcntiun : — the society of naturalists (founded in 1805) ; the
eocietj' of Kuasian history and antiquities, which has published
many remarkable worksj the society of amateurs of Russian litera-
tiuw ; the physical and medical society ; the mathematical society ;
tho society for the dilTusion of useful books ; the very active arcluoo-
logical society, founded in ISSl ; a society of gardening and of
agriculture ; several technical, artistic, and musical societies ; and
the very active young society of the friends of natural science, which
already has published many useful volumes.
Among the museums of Moscow, the musenm, formerly Buman-
tseffa, now connected with the so-called "public museum," occupies
the first rank. It contains a library of 160,000 volumes and 2300
MSS. , remarkable collections of old pictures, sculptures, and prints,
aa well as a rich mineralogicsl collection, and an ethncgrapliical
collection representing very accurately the various inhabitants of
Russia. Tho historical museum has already been mentioned. Tho
private museum of Prince Golitzyn contains a good collection of
paintings and MSS. ; and great treasures of archeology are amassed
in various private collections in Moscow and its suburbs.
The periodical press does not on the whole exercise great influ-
ence ; twenty-five periodicals are published, besides those of scientific
societies. But Moscow publishes a far larger number of books for
primary inati-uciiou and of the humblest kind of literature and prints
for the use of peasants than any other Russian city,
. The philanthropic institutions are numerous, the first rank being
occupied by the immense Foundlings' Hospital, erected in 1764.
The nospitals, municipal, military, and pri\'ate, are very large, but
much below the standard of other capitals. The number of private
philanthropic institutions is very considerable.
Though the drama was introduced into Russia at Kieff, Moscow
was the place of its development. The earliest stage representations
were made at Moscow in 1640, and the first comedy — a translation of
iloVi^.re'aSfddecmAfcUip-^Lui — was played in the palace before Sophie,
tho sister of Peter I. It was only in 1769 that a theatre was erected.
A lar.ge stone theatre was erected in 1776, and rebuilt in 1856 after
a fire. It is for the Moscow stage that the best Russian dramas
have been written, and it was in the " small theatre " that the best
Russian actors — Schepkin, Sadovsky, Shumsky, and Madame Va-si-
lieff — exhibited the comedies of Gogol, Griboyedolf, and Ostrovsky.
Moscow, where the Great-Russian language is spoken in its
graitest purity, was the bii'thplace of the two chief Russian noets,
Pushkin and Lermontoff, as well as of Griboyedolf, Ostrovsky, and
Hcrzen. A monument to Pushkin was erected in 1880, on the
Tverskoy boulevard. Griboyedoff, in his remarkable comc^ly Gori
U siijw, has given a lively picture of the higher Moscow society of
the beginning of this century, which continued to hold good until
within the last few years. His remark as to the unmistakable
individuality of the Moscow type also maintains its truth ; although
the physiognomy of Moscow has much changed since his day, it
Btill h.os its special features that distinguish it from every other
capital. The division of classes is much more felt at Moscow than
elsewhere. The tendency towards m-iginality, the love of grandiose
undertakings, a kind of brag, together^ with little feeling of inde-
pendence, a good deal of laziness, and much cordiality, still charac-
terize the educated classes. The merchants live quite aloof from
any political or even intellectual movement, under a rude patri-
archal system, well described in the dramas of Ostrovslcy. A large
proportion of them are nonconformists. Their sons, the weS-
Known kupecheskiye synki, "merchants' sons," when they leave
this kind of life, astonish tho capital witli their extravagances and
absurd display of wealth. But Moscow takes its present phj-siog-
nomy chiefly from its busy lower classes. The streets aro full of
merchants and peasants, who continue to wear the old Ruasian garb,
go on foot in the sti-ects, drink tea in modest restaurants, and trans-
act large business. From being a town of the aristocracy, Moscow
is coming to be more and more a torni of the wealthy middle
classes, who persist in keeping the low educational level of tho
peasants in the villages, ana have but one aspiration, to beoome in
their turn "merchants" of tho t>'pe described by Ostrovsky.
Suburbs. — iloscow is suiTOunded by beautiful parks and pictur-
esque suburbs. Of the formerone of the most frequented is the Petior-
eky Park, to the north-west. A little farther out is the Pctrovskoye
llaziunoyskoye estate, with an agricultural academy and its do-
pndencies (boUinical garden, experimental farm, &c.). Another
largo park and wood surround an imperial palace in the village
of Ostankino. Tho private estates of Kuzminki, Kuskovo, and
Kuntzevo are also surrounded by parks ; the last has remains
of a yery old graveyard, supposed to belong to the pagan period.
Twenty-eight miles westward from the city is the Sawin-Storojevsky
monastery, situated, like so mnnyother Russian monasteries, jn a very
fertile country, amidst beautiful forests ; it has a pretty cathedral,
a rich treasury, and library. Farther westward still is the New
Jerusalem monastery erected by the patriarch N.ikon.
In the south-west, on the right bank of the Moekva, which hero
makea a great bend to the south, are the Vorobiovy hills, which
are accessible by steamer from Moscow, and afford one c\f tho best
views of the capital. In the bend of the Moskva is situated the
Novo-Dyevitchiy convent, erected in 1525, aud connected with
many events of Russian history. It is now tKs burial-place of tho
Moscow aristocracy, and one of the richest nunneries in Russia. The
village Arkhangelskoye has also a good park and a palace built by
RastreUi. Iliynskoje, formerly a private estate, was purchased by
the imperial family in 1864.
In the south, on the road to Sorpukhoff, is the village of
Kolomenskoye, the residence of Alexis Mikhailovitch, with a
church built in 1531 (a striking monument of Russian architecture,
restored in 1880). Diakovo has also a church built in the 16th and
17th centuries — a pure example of the architecture of Moscow,
recalling the temple of Vasili Blnjennyi. One of the best sites in
the neighbourhood of Moscow is occupied by the park of Tsaritzyno
(11 miles from the Eur^ railway^jtation), purchased by Catherine
II., with an unfinished palace ard a beautiful park. The monastery
Nikolo-Ugryeshskiy, 12 miles from the city, between the Kursk
and Ryazan railways, also occupies a beautiful site, and is much
visited by Moscow merchants, to venerate a holy picture by which
Dmitry Donskoy is said to have bejn blessed before going to fight
the Mongols.
In the north, the forest of Sokolniki, covering 4 J squai^ miles,
with its radial alleys and numerous summer residences, is the part of
Moscow most frequented by the middle clnsses. Close by, towards
the east, is situated the Preobrajenskoye suburb, the centre of the
nonconformists, and farther south tho village of Izmailovo, with a
home for invalids and a model farm for apiculture. To the west
of Sokolniki is situated the wood of Mariiua, the favourite resort
of the merchants and " merchants' sons," who there spend fabulous
sums of money on choirs of Gipsy singers.
Hialory. — Tlie Russian annals first mention Moscow in 1147 as a
place where Yuri Dolgoruki met with Svyatoslav of SyeveWk and
his allies. The site was inhabited from a very remote antiquity
by the Merya and Mordviuians, whose remains are numerous in
the neighbourhood, and.it was well peopled by Great-Russians in
the 12th century. To the end of the 13th century Moscow re-
mained a dependency cf the princes of Vladimir, and fiad to suffer
from the raids of the Mongols, who burned and plundered it in
1237 and 1293. It is only under the rule of Daniil, son of Alex-
ander Nevsky (1261-1302), that tho prince of Moscow acquired
some importance for the part he took in tho wars against the
Lithuanians. He annexed to hia principality Kolomna, cituatod
at the confluence of the Moskva with '.he Oka. His son in 1302
annexed Pereyaslavl Zalcssky, and next year Mojaisk (taking thus
possession of the Moskva from its head to its mouth), and bo
inaugurated a policy which lasted for centuries, and consisted in
the annexation by purchase and other means of the neighbouring
towns and villages. In 1300 tho Kremlin, or fort, was enclosed
by a strong wall of earth and wood, offering a protection to nu-
merous emigrants from the Tver and Ryazan principalities who
went to settle around the new city. Under Jolin Kalita (1325-
1341) the principality of Vladimir — where tho princes of Kieff
and the metropolitan of Russia had taken refuge after the wars
that desolated south-western Russia — became united with Moscow ;
and in 1325 the metropolitan Peter established his seat at Moscow,
giving thus a now importance and a powerful support to tho young
principality. In 1367 tlie Kremlin was enclosed by stone walls,
which soon proved strong enough to resist the Lithuanians under
Olgerd (1368 and 1371). Tin son and grandson of Kalita steadily
pursued tho same policy. The latter (Dmitry Donskoy) annexed
the dominions of Starodub and Rostoff, and took pai-t in the re-
nowned battlo of Kulikovo (1380), where the Russians ventured for
the first time to oppose the Mongols in a great pitched battle.
Tho church, which strongly supported the princes of iloscow,
ascribed the presumed victory to him and to the holy pictnres
of the Moscow monasteries.
At this time Moscow occupied a wide ai-ea covered with villages.
The Ej-emlin had tliree cathedrals-^ld, small, and dark buildings,
having narrow ■u-indows filled ivith mica-plates — which were sur-
rounded by the plain wooden houses of tho prince and his boyara.'
To the east of the Ki-cmlin was \h^ posad, or city, also enclosed by
a wall, and even then an important centre |^ trade. Different
parts of the town belonged to different princes. 1^ 1366 Moscow suf-
fered from pestilence. Two years after the battle df Kulikovo it was
taken and plundered (for the last time) by the khan (Toktamish),
The gradual increase of the principality continued during the
first half of the 15th century, and at the death of Vasili II. the
Blind, in 1462, it included not only the whole of what is now the
government of Moscow, but also large parts of the present govern-
ments of Kaluga, Tula, Vladimir, Nijni - Novgorod, Kostroma,
Vyatka, Vologda, Yaroslav, and Tver. Still the prince, although
assuming, like several others, the title of Great Prince, had simply
860
M O S — M O S
a littlo mftrc influence than other independent rulers in the affairs
of north-eastern Russia, and was recognized as the eldest prince
by the khans. The towns which reco^^nized his supremacy were
<iuite independent, and only paid to his representatives the judi-
ciary taxes, in exchange for military protection. It is only under
Ivan HI. {called the Great by some Russian historians) that the
prince of filoscow asserted his claims on other parts of Russia, and
called himself "Ruler of all Russia" (Hospodar vseya Rosii). It
was about this time, when the wealth of Moscow was rapidly in-
creasing by the extension of its trade, that the embellishment of
the town began. In room of the old cathedral Uspensky, a new
structure was built by Fioraventi of Bologna, aided by -Novgorod
masons. The cathedral Arkhangelsky was also rebuilt, and a third,
lilagovyeschensky, was erected, as well as a stone palace and other
buildings. The Kremlin was fortified by strong towers, and the
houses and churches built close to the walls were destroyed. In
1520 Moscow was said to contain 45,000 houses and 100,000 in-
habitants. Its trade was very active. Ivan IV. finally annexed
Novgorod and Pskov to ^loscow, and subdued Kazan and Astra-
khan. But after this reign Moscow suffered for a long time a
series of misfortunes. In 1547 two dreadful conflagiations destroyed
nearly all thn city, and a few days later the khan of the Crimea
advanced against it with 100,000 men. He was compelled to retire
from the banks of the Oka, but in 1571, taking advantage of the
state into which Russia was brought by the extravagances of Ivan,
ho took JIoscow and burned all the town outside the Kremlin.
The gates of the Kremlin having been shut, thousands of people
died in the flames, and the annals record that of the 200,000 who
then formed the population of Moscow, only 30,000 remained. In
1591 the ]\Iongols were again in Moscow and avenged their repulse
from the KicniHu en the inhabitants of the open town.
By the ead of t.ho 16th century Moscow was a large city, not
less than 14 miles in circumference. The " Great Posad," or city,
containing :ieveral Gostinoy Dvors for merchants of all nationali-
ties, was enclosed in 1534 by a trench and stono wall, which
still exist The " White Town " which enclosed the Kremlin and
Great Posad from west and north was also fortified, in 15S6, by a
stono wall (ilcstroyed in the ISth century) ; and in 15S3 a third
enclosure, a ;>alisaded earthen wall, the Zemlyanoy-Gorod, was begun,
including all the town that surrounded the three former subdivi-
sions ; it remained until the end of the 18th century. Foreigners
who visited Moscow spoke with astonishment of its wealth and its
beauty. But tlie internal aSairs of the capital were in very bad
case. During the century, oaring to the increase of population,
new annexai ions, and a lively trade, the power of the boyars had
gradually increased. The peasants who settled on their lands, or
on the estates of the prince given to boyars, had gradually become
their serfs ; and the political tendency of the boyars, suppotted
by the wealthier middle classes (which had also a rapid develop-
ment in tlK same century), was to become rulers of Russia, like
the noblesse of Poland. During the reign of Theodore, Boris
Godunoff, the regent, ordered the murder of the heir to the throne,
Demetrius, son of Ivan IV,, and himself becamo czar of Russia.
Moscow suffered severely in the struggle which ensued, especially
when the populace rose and exterminated the Polish gamson, on
which occasion the whole of the town outside the iCremlin was
again burned and plundered. But in compensation it had acquired
in the eyes of the nation a greatly-increased moral importance, as
a stronghold against foreign invasions. The monastery of Troitsa,
■which the Poles besieged without taking, was invested with a
higher sanctity. The touii also by and by recovered its commercial
importance, and this the more as other commercial cities were
ruined, or fell into the hands of foreigners ; and thirty years after
1612 LIoscow was again a wealthy city. O^nng, however, to the
ever-increasing concentration of power in the hands of the czars,
and the steady development of autocracy, it lost much of its
political importance, and assumed more and more, especially under
Alexis Mikhailovitch, the character of a private estate of the czar,
its suburbs becoming mere dependencies of his vast household.
During the whole of the 17th century Moscow continued to be
the scene of many troubles and internal stniggles. The people
fccveral times revolted against the favourites of tlie czar, ana were
subdued only by cruel executions, in which the sircltzy — a class
of citizens and merchants rendering hereditary military service —
supported the czar. Afterwards appeared the rasJcol or noncon-
fonnifit movement, and in 1648, when the news spread that Stenka
Razin was advancing on Moscow "to settle his accounts with the
boyars," the populace was kept from rising only by severe repres-
sive measures and by the defeat of the invader. Later on, the
sfreltzy themselves engaged in a scries of rebellions, which led the
youthful Peter I. to shed rivers of blood. The opposition encoun-
tered at Moscow by his plana of reforming Russia according to his
ideal of military autocracy, the conspiracies of the boyars and mer-
thants, the distrust of the mass of the people, all compelled him
afterwards to leave tlie city, and to seek, as his ancestors had
done, for a new capibil. Tliia he founded on the very confines of
the ni^itary empire he was trying to establish.
In tho course of the 18th century Moscow became the s^at of %
passive and discontented opposition to the St Petersburg Govem-
raent. Peter I., wishing to see Moscow like other capitals of westera
Europe, ordered that only stone houses should be built within th<
walls of the town, that tho streets should be paved, and so on ;
but his orders were only partially executed. In 1722 the Kremlin
was restored. In 1739 the city becamo onca more the prey of »
great conflagration ; two others followed in 1743 and 1753, anff
gave an opportunity for enlarging some streets and squares; In
1755 the first Russian university' was founded at Moscow. Catherine
II. tried to conciliate the nobility, and applied herself to benefit
the capital with new and useful buildings, such as the senate hous^
the foundlings' and several other hospitals, salt stores, ice Tho
cemeteries within the town ayere closed after the plague of 1771 ;
several streets were enlarged, and the squares cleared of the email
shops that encumbered them. Water was brought by an aqueduct
from the Mytischi villages. In 1787 the city had 303 churches, 24
monasteries and convents, 8965 houses (of which 1595 were ofstone^
one printing-ofiice, and 314 manufactories and larger workshops;.
The last public disaster was experienced by Moscow in 1812. On
13th September, six days after the battle of Borodino, the Ruseiaa
troops evacuated Moscow, leaving 11,000 wounded, and the next
day the French occupied the Kremlin. The same night, while
Napoleon was waiting for a deputation of Moscow notables, and
received only a deputation of the rich raskohiik merchants, th«
capital was set on fire by its own inhabitants, tho Gostinoy Dvor,
with its stores of wine, spirits, and chemical stuffs, becoming the
first prey of th-j flames. The inhabitants abandoned the city, and
it was pillaged by the French troops, as well as by Russians them-
selves, and the burning of Moscow became the signal of a general
rising of the peasants against the French. The want of supplit-a
and the impossibility of wintjoring in a ruined city, continually
attacked by Cossacks and peasants, compelled Napoleon to leave
JIoscow on 19th October, after he 1^ uusuccesaftUly tried to blow
up- certain parts of tho Kremlin. (P. A. K.)
MOSELLE. See Rhin-e.
MOSER, JoHAifN Jakob (1701-1785), jurist, xvaa boro
at Stuttgart on 18th January 1701. He studied at tlo
university of Tubingen, Tvhere, at the early age of idnet€€:i,
be became professor extraordinarius of law. A year later
bo resigned his chair, with the expectation of receiving an
appointment at Vienna, but tliia was refused him on his
declining to join the Catholic Chiu-ch. From 1729 he
for some years held an ordinary professorship of law at
Tiibingen, and in 1736 he accepted a chair and directorship
in the university of FrankfortHDu-the-Oder. On account,
however, of differences with King William I. of Prussia,
be resigned these in 1739 and retired to Ebersdorf, a village
in the principality of Reuss, where for several years be
devoted himself wholly to study, and especially to the
production of bis Deittsches StaatsrecJU. Jn 1751 be was
called back to Wiirtemberg as 'Mandscbaftsconsulent,*
and in 1759 was imprisoned at Hobentwiel on account of
the steps be bad taken in connexion with this office against
certain tyrannical proceedings of the duke.. In 1764 ho
received bis liberty and was restored to office, but from
that time took little part in political affairs. He died 30tli
September 1785.
Moser was the first to discuss in an adequate form the subject of
European international law, and he is the most voluminous German
writer on public law. In oU, he \vrote more than 500 volumes,
his principal works being Dcuisches Staatsi'ccht^ 1737-1754 ; 2seuei
Dcutsckcs S(aalsrcch(,l7QQ-'L775 ; Deutsches Staatsarcldv, 1751-1757;
Griindriss der keutigoi StnaUvcrfassitng von DctUschland, 1764.
See Schmid, Daa Leben J. J. Moser's, 1S6S ; Schulzc, J. J. Moter,
der V'atcr dcs Dcutschen Siaatsrechts, 1869. ■
MOSES. Of the life of Jtloses we have few certaia
details, though the bistory of Israel bears witness to the
import^ance of bis worlc To what has been said under
IsR.vEL there will here be added a brief summary of what
has been banded down about him. His origin and the
bistory of his cbildhood can be read in Exod. i., ii (comp.
vi. 16 sq.)-y the statements there given are enlarged and
modified in the Jewish Midrash, particularly as we find it
in Josepbus and Philo.^ The daughter of Pharaoh, we are
told, was called Thermutis (Ant.^ ii 9, 5), or Merris (Euseb.,
1 In still more fantastic form in tho Psleatiniftn Taigiun on Exodus^
the details of which neoil not be r^petted hare.
MOSES
861
Trtip. ^., ix. 27) ; die named the boy Moiwr^s, not because
she used the Hebrew verb mm to express the fact that he
was drawn out of the water, but because the Egyptian word
for water wis ma, and iwijs applies tc those who have been
delivered from it (^re<., ii. 9, 6 ; comp. Philo, ed. Mangey,
ii. 83 ; Euseb., I.e.', ix. 28). She took care to have hiin
trained in all the wisdom of the Egyptians (Acts vii. 22)
and in that of the Greeks, Assyrians, and CUaldaeans as
well (Philo, ii 8i). To his great intellectual endowments
eorresponded his personal beauty, of which Josephua speaks
in extravagant terms {Ant., ii 9, 6-7). It was on account
of this beauty that, when on one occasion, as a young man,
he led an Egyctian army against Meroo, the Ethiopian
princess Tharbis opened the gates of the capital to him in
order to, make him her husband {Ant., ii. 10; comp. Numb,
xii. 1). '
For reasons explained in Exod. ii. 11 so., Moses Vii
the land of Pharaoh and came to Midian to the Kcnite
priest Jethro (also called Hobab Ben Eaguel and Raguel),
whose daughter Zipporah he married, becoming by her the
father of two sons, Gershom and Eliezer (Ezod. ii. 21 tq.;
xviii. 2 »q.). During his stay in Midian he received, at
the foot of Sinai (Horeb), the divine revelation at the
burning bush whereby he was called to become the liberator
of Isriel from Egyptian bondage. With much reluctance
be at last accepted this vocation, and, already expected by
his brother Aaron and the elders, returned to his people.'
Arrived in Egypt, he associated Aaron with him as his
interpreter, being himself no orator, but a man of counsel
and action, and appeared before Pharaoh to demand of the
king in Jehovah's name permission for the people to go with
flocks and herds into the wilderness to celebrate there a
festival (the spring festival of the Passover) in honour of
their God. Jehovah gave emphasis to the demand by
great signs and wonders, — the plagues of Egypt, which have
their explanation for the most part in evils to which Egypt
ia periodically liable, but are treated by Israelite tradition
as the weapons of Jehovah in his ever-intensifying conflict
with the king and the gods of Egypt. At length, by the
slaying of the first-born, the stubbornness of Pharaoh was
broken, so that he consented to, and even urged, the de-
parture of the Hebrews. By and by, however, he changed
his mind, and, setting out in pursuit of the Hebrews, over-
took them at the Red Sea ; but Jehovah fought for them,
and annihilated Pharaoh's chariots and all his host. In
order to present themselves in proper festal array at the
celebration for the sake of which they were going into the
wilderaess, the Hebrew women had borrowed dresses and
ornaments from those of Egypt ; the Egyptians could now
only blame themselves and their hostile conduct if those
articles were not returned.'
By the miracle wrought at the Red Sea Moses was
pointed out to the Hebrews as the man of God, to whom
accordingly they now committed the task of caring for
thi ir outward life as well as their spiritual guidance. He
led them first to Sinai, where the law was revealed and the
worship in connexion with the ark of the covenant insti-
tuted. When he had communed face to face with the
Godhead for forty days on the holy mountain, the skin of
his face shone so that he had to wear a veil (hence the
boras, properly rays, on his forehead). Driven irom Sinai
in consequence of their worship of the golden calf, the
Israelites removed to Eadesh with the view of entering
> Od the road occurred the remaikable incident which, in the view
of the narrator, led to the circumcision of infants being substituted
foi that of the bridegroom (Eiod. i7. 21, 25 ; \hyh Wni, to mark
the suUtitution, — compare the euphemism in Isa. viL 20).
' Quite contrary to the sense of the Biblical narrative, Justin (xxrvt
S, 13) says, " Sacra iEgyptiorum furto abstulit ; " and still more per-
verse is tb« glosa which £wald, proceeding spoB tliil upreuion of
i^utiQ, givea.
Palestine. But this plan was defeated by their unbelief
and faintheartedness, and, aa a punishment, they were
compelled to sojourn forty years in the wilderness of Eadesh
(Paran, Sin). It was here and now that the people went
to school with Moses ; here, at the sanctuary of the camp,
he declared law and judgment; and here, according to
the view of the oldest tradition, the foundations of the
Torah were laid (Exod. xviii.). The region of Eadesh
was also the scene of almost all- the miracles and other cir-
cumstances we read about Moses. Here he showed himself
to be at once the father and mother of the people, their
judge, priest, and seer. It was not till towards the very
close of his life that he led the Israelites from Eadesh into
northern Moab, which he wrested from the Amorite king,
Sihon of Heshbon, Here he died on Mount Pisgah or
Nebo, after taking leave of the people in the great legisla-
tive address of Deuteronomy. According to Deuteronomy
xxxiv. 6, he " was buried in a valley in the land of Moab,
. . . but no man knoweth of his sepulchre unto 'Jiis day." '
As his successor in the leadership, Moses had named Joshua
ben Nun, but -the real heirs to his position and influence
were the priests at the sanctuary of the ark of the covenant.
Of his personal character the Bible tells us nothing (for
UV in Numb. xii. 3 means orJy " heavily burdennd ") ; but
'later Judaism is all the more at liberty on this t.ccount to
expatiate upon it (see especially Josephus, Ant., iv. 8, 49).
Such in brief r^3Umi are the accounts of Moses given in the Bible*
and the Midrasb. In addition to these we have also the statementa
of Hellenistic writers, preserved chiefly in the Contra Apionem of
Josephua. These are all of an Egyptian complexion, an 1 pi'obably
embody no ancient and independent tradition, but, in all that
relates to the Hebrews, where they do not rest upon pure conjec-
ture, merely go back upon obscure rumours of .Jowiah origin and
dress them up after the manner of the Midrash — only in a con-
trary sense, with hatred and not with love — and then seek to fit
them aa well as may be into the Egyptian history and chronology
as known from otlier sources. The great number of new proper
names of places and persona which occur in the writings of Manetho
and his like cannot be urged against this view, for the Midrash also
is full of them. The very name Osarsiph, given to Moat>3 himself,
moreover, suggests a suspicion of dependence on the Asaphsuph,
"mited multitude" of Numb. xi. 4 (comp. Exod. xii. 36) ; wnat
is said in these places is known to have played a great part in th»
rise of the idle Egyptian tales about the origin of the Jews and of
their lawgiver.
For literature, see the varions commentaries on the Pentateuch,
end especially DUlmann on Exodus. (.1. WE. )
MOSES OP Choeene was a native of Ehor'ni * in Tarfln,
a district of the Armenian province of Turuberan. Accord^
ing to the only trustworthy" authority — the Hktort/ o/
Armenia^ which bears his name — he was a pufil of the
two fathers of Armenian literature, the patriarch or catho-
licos Sahak the Great and the vartabed Mesrdb. Shortly
after ^31 he was sent by these men to Alexandria to study
the Greek language and literature, and thus prejjare hiln-
self for the task of translating Greek writioga into
Armenian. Moses took his journey by Edessa and the
sacred places of Palestine. After finishing his studies in
the Egyptian capital lie set sail for Greece ; but the ship
was driven by contrary winds to Italy, and he f.eized the
opportunity of paying a flying visit to Rome. He then
visited Athens, and towards the end of winter (440) arrived
in Constantinople, Whence he set out on his homeward
journey. On his arrival ia Armenia he found that hi»
patrons were both dead. The History of Arvunia speaks
of its author as an old, infirm man, constantly -mgaged in
the work of translating ' In the later Armenian tradition
• The legend of his assumption is of later growth ; see Vie apocryphal
Atsvtmptio Moysis (Apooalyttio Lttkbatdse, vol ii p. 177), and
compare Luke ix 30, 33 ; Jude 9.
• Outside of the Hexateuch, however, he is almost nei er raentianed.
• Ct Sukias Somal, (^uadro dtUa itoria letteraria di Armmia, p»
U tq. ' 'ii- 61 't-i 68, 66.
' On linguistic grounds, the Uechitarists ascribe to hun the ttuuUr
ttOB of £aseblua'i Chrmide and of the Pwudo-CaUistb'iuei,
862
■we find other notices of this celebrated man,^ — such as,
that he was the nephew of Mesr6b, that he \ras publicly
complimented by the emperor Marcian, that he had been
ordained bishop of Bagrewand by the patriarch Giut, and
that he was buried in the church of the Apostolic Cloister
at Mush in the district of Taron ; but these accounts must
be received with great caution. This reniark applies
especially to the statement of Thomas Ardsmni,- that
MCises, like his Hebrew prototype, lived to the age of 120
years, and recorded his own death in a fourth book of his
great work.' The same caution mast be extended to
another tradition, based on an arbitrary construction of a
passage in Samuel of Ani,* which places his death in the
year 4S9.
Of the worts of Moses ' the best known is the History
of Armenia,^ cr, as the more eitct title runs, the Genedlogi-
cal Account of Great Armenia. It consists of three books,
and reaches down to the death of Saint Mesr6b, in the
second year of Jazdegcrd II (17th February 440)." It is
dedicated to Sahak Eagratuni (who was afterwards chosen
to lead the revolted Armenians in the year 4S1), as the
man under whose auspices the work had been undertaken.
This work, which in course of time acquired canonical
authority among the Armenians, is partly compiled froiji
sources which we yet possess, viz., the Life of Saint Gregory
by Agathangelos, the Armenian translation of the SjTiac
Doctrine of Ute Apostle Addai, the Antiquities • a.\idi the
Jewish ITar of Josephus, and above all the History of Mar
Abas Kalina (still preserved in the extract from the book
of Sebeos),* who, however, did not write, as Mtises alleges,
in Syriac and Greek, at Nisibis, about 131 B.C., but was a
native of Medsurch, and wrote in S)Tiac alone about 3S3
i.D., or shortly thereafter. Besides these, Moses refers to
a whole array of Greek authorities, which were known to
him from his constant use of Eusebius, but which cannot
possibly have related aU that he makes them relate.'
Although Moses assures us that he is going to rely entirely
upon Greek authors, the contents of his work show that it
is mainly drawn from native sources. He is chiefly indebted
to the popular ballads and legends of Armenia, and it is
to the use of such materials that the work owes its perma-
nent value. Its importance for the history of religion and
mythology is, in truth, very considerable, a fact which it
is the great merit of Erain '^ and Dulaurier >' to have first
pointed .out. For political tistory, on the other hand, it
it of much less value than was formerly assumed. In
particular, it is not a history of the people or of the
country, but a history of the Armenian aristocracy, and, in
MOSES
1 Collected by Langlois, Collection dcs Jtistoriens de VAnyi^ie^ ii.
5 In Erosset, Collection d^hisioricns Arm/niens, i. 63.
' There is not tlie tUgUtest allnsion elsewhere to any snch book.
• lu Erosset, ii. S87.
• Complete edition of the Mechitiirists, Venice, 1843 ; new ed.,
T865, 8ro.
« The oldest MS. "is tbat of S. lanih of the 12th c-entory. Col-
lutjons of MSS. of Etchmiadzin imd Jemsilem are given by Agop
Gahsia^ 15818, 1 85S, 4to. The book has been edited and translated by
WTiiston, London, 1786, 4to ; and by Le Yaillant de Florival, Venice
and Paris, s-a. (1841), 2 vols. Svo.
' The commencement of this king's reign has been fixed by Noldeke
(Oeschiehte dcr S^xxniden atis Tahari, p. 42S) as 4th August 4SS ;
and this date has subsequently, been established by documentary
evidence from the fi^ct of the martyrdom of Petbion (see Bofiinaan,
.AHsxiiffe aus SyrwcA.f ^ AlUin prrsischer M&rtyrer^ p. 67),
• Translated in Lrjgloit, i. 195 a;. —
• For the followLrg statements, the proofs may be fonnofi the
article " Ueber die Ckubwurdigkeit der Aimeniscben Geschichte des
Moses Ton Khoriia," by the present writer, in the Bmc}ii£ der jthil.
hisior. Ciaste dcr lUjni^l. Sitchs. Oetellsck^fl der Wissenschj^flen^ 1876,
P- 1 »?• \ ;>
" r*c £jn{ SmJIi c/ Ancient Annenia (Arm.), Moscow, 1850.
^ *' £tudes Eur lea chants historiqces et los traditions populaires de
I'lsdens* Anaisle," is the Jeum. AtiaL, Ir., air. It (1S52), p. S f ■
opposition to the Mamikonian tendency which pcrvade&'flit
rest of the older Armenian historical literature, it is written
in the interest of tie riTdl Eagratunians. Down to the 3d
century it is proved by the contemporary GrsTCO-Komaa
annals to be utterly untrustworthy ; but cven'for the times
of Armenian C!hri£tianity it must be used far more
cautiously than has been done, for example, by GibboiL
The worst feature is the confusion in the chronology, which,
strange to say, is most hopeless in treating of the con-
temporaries of Mosea himself. 'What can be thought of a
writer who assigns to Jazdegerd L (399-420) the eleven
years of his predecessor Bahrtai FV., and the twenty-one
years of Jazdegerd I. to his successor Bahrdm V. (420-439) t
The present writer ^ formerly attempted to explain this
unhistorical character of the narrative from a tendency
arising out of the peculiar ecclesiastical and political cir-
cumstances of Armenia, situated as it was between the
eastern Koman and the Persian empires, circumstances
which were substantially the same in the 5th as they were
in the two following centuries. In the course of further
investigations, however, he has come to the conclusion
that, besides the many false statements which Moses of
Khor'ni makes about his authorities, he gives a false
acooimt of himself. That is to say, the author of .tha
History of Armenia is not the venerable translator of the
5th century, but some Armenian writing under his name
during the years between 634 and 642. The proof is
furnished on the one hand by the geographical and ethno-
graphical nomenclattire of a later period and similar
anachronisms,^^ which nm through the whole book and are
often closely incorporated with the narrative itself, and on
the other hand by the identity of the author of the History
with that of the Geography, a point on which all doubt b
excluded by a number of individual affinities,^' not to speak
of the similarity in geographical terminology, llie^critical
decision as to the authorship of the Geography settles the
question for the History also.
The Geography is a meagre sketch, based mainly on the Chcro-
gmphy of Pappus of Alexandria (in the end of the 4th century),
and indirectly on the work of Ptolemy. Only Armenia, the Persian
empire, and the neighbouring regions of the East are independently
described from local information, and on these sections the valne
of the little work depends. Since the f.jst published text ^ contains
names like ' ' Sussians " ancj "Crimea, " Saint Martin in his edition "
denied that it was written by Mdscs, and assigned its origin to th»
10th century. It was shown, however, by L. Indjidjean •" that
these are interpolations, which are not found in better manuscripts
And in fact it is quite evident that a book which gives the division
of the Sasanid empire into four spahbehships in pure old Persian
names cannot possibly have been composed at a long interval aft«r
the time of 'the Sasanidsa. But of course it is equally clear that
such a book canuot be a genuine work of Moses of Khor'ni ; for
that division of the empire dates from the early pait of the reign
of King Chosran I. (681-579)." Accordingly the latest editor, K.
P. Patkanow," to whom we are indebted for the best text of ths
« "Ueber die GlnubwUrdigkeit, " &c, p. 8 sj.
" Instances of these may be found in i 14, where the arrangement
of Armenian provinces I., II., HI., IV., introduced in the year 536, ii
carried back to Aram, an older contemporary of Niuus ; and in tha
passage iii. IS, according to which Shipto IL penetrated to E.thynia,
although the Persians did not reach that till 60S.
" See the confusion, common to both books, between Cappadocia I.
and Armenia I., in consequence of which Maralca and Mount ArgXus
are transferred to the latter locality {HisL, 1. 14 ; <3eogr., Saiut Martin'i
ed., ii. p. S54) ; also the passages which treat of China and Dchenbakur
{Bisl., ii. 81 ; Gco^., ii p. 876), &c
" Edition with translation by Whiston, London, 1736, 4to.
>• In the ilimoires histori^uet et gdigTaphigves sur tArmtnie (PuH
1819, Svo), ii. p. 301 tq.
" Antiquities of Armmia (Aim.), iiL p. 303 <}.
" See Noldcke's Tdhari, p. 155 «g.
" Armiansluiji gtOfraph>}a ni. w&iapo T. Ch. (pripisiw awscbljaqk
Moiseju ichorenskomn), St Petersburg, 1877, Svo. Before him
Kiepert (in the lianaxA. d. Berliner Akad., 1873, p. B99 sq.) had
substantially arrived at the right conclusion when be assigned tha
portions of the Geography tsferring to Armenia to the time betvtea
Justiitiaii and Mauhoa.
be regarded *t s tt
Siullerirorke I- :
teSalzJ^Jrirr.--,:
•a.
M O S-
Otojnoky, it of pfinicia fi« rm luTt in it s »riti=p rf tlie Tti
eeiita*7. In (hit jadj;muit i>« bxmX txmaa; aad, if tie IbsiU
■uitii'l Triiicli tte Gro^myi.y was oompoied an to be more nearlr
ieirti, vt may ca.T tL^t, ffiu u'^lated tzaoeiof Arab mle' (irliicli
in A^meiiiA dates £rom C^l), it nmst here been vzittea oerUinlj
aflBr tlst jeu-, and peiiianB aboot Ilia year C57.'
Another eztasi iroi-k cf Uosea ia a iliaial cf Shdarie, in ten
booka, dedicated to his pnral TfaeodoniE. It is dnm ap after
Creek modela, is tie taste of tie rbetone and eonUatiy of tiie later
bspeiial period. The examplea are takes froa aamogtatm, Theon,
Apiitlkonuic, and Libanioi ; altloa^ tie ajthor ia alao aeqnaiatod
vitli loat wiittnet, eg., tie FiUadti, eS Euripidea. On aewnat tt
tie diTeqpeaoe « it* ctfla Cnm diat of tie Batmrf tf Armemia,
ArmeaiaB adiolai*' bave ImmIiIiiiI to aacribe tie BJuiaric ta Moaea
of Ebtn'm : bnt, fnmi irhut hat brt n uid aboTC, tlia ia rt&a to
-rdty.
'J cured name ' are^tiae JjtAXtr
:/ c Hol-y Jiiffthcr vf God and her
a in the distiict Asdaerata of
. J5 ales addnaeed to Salak ;
'-. Of tie aacnd poena atti-i-
'T T-jivT rnr.t^mcd in tie
■ -.T,
-•Iloir.
tt; . liiit
ti- :: aad
a] . G.)
^: 1T;.5), wen
kn-- r. .ished in Ilia
dav i.; :. : _ „_beek on the
9t!i of OcU>l>£x. X^crs it, soius -..r..-^nj.ir.ij.- as to the J'ear,
but tLe probabiJity b in faxonr of 1693 or 1694. He
received a Eomewhat irregular education at the gymnasinm
of his native place, and afterwards entered tie nnireis^
of Kiel, -n-here he took his master's degree in 1718. Hu
£rr- : :-j the field of literature vas in a potaiiHjJ
tri 1 i, VtHdicite ajUijtue Clirittiamoram dit-
<il-: ^ch tras soon foUoved bj *. Tolnme of
OU^rr:',. . ■ i : .r (1721). These voffa, along vilb the
Teput:itiDn Le li^d c; quired as a lecturer on jAaioaof^j,
and al:-o ls a f<.Tvcnt i^d eloquent preacher while acidng
as assiftant to Aibrcclit z:im Felde, his teacher and future
fatber-in-latr, Bemred for him a caH to a theofe^eal chair
at Helmstadt, in 1723. The iHflifKtic^trm ffitlarim Eixte-
fiaeticx hbri IV. appeared in 1726 (2 toIs., 12mo), and
in the same jear he -n-as appointed by the duke of Bruns-
wick abbot of Marienthal, to which dignity and eoMiIa-
ment the abbacy of MichaehteiQ xras added is the ft^lawing
year. Mo^Ltim T-as much consulted by the antfaoritieB
tL. " !ver£Jty of GOttingen was being formed;
esj to do trith the framing of the statntes
of ■ ] faciJty. and with the proviakms for
mail Mdent of the eodesiastaeal
conn " . :. 1726 a pctsnise to resnaiB
in K:.. .■.;.:•. _. _! -:,:.:: to accept the call to the
Georgia Auguita iTiiich was urgently pressed npon birn^
tmtil the year 1747, when the duke of Brunswick at last
released him from Us obligation. To enhance the dignity
he already possessed as a learned and brilliant theological
professor at Guttinren. a new oSce was specially created
for him, that of cl : h, however, proved some-
what bnrJaisome alousy of tie nobles whom
he governed. E- lingen on 9th Septeaiber
il o s
863
tad gntdli
* ne raaaase abaat fha trade of Btsnh, vlidi was f onaded i>6>5,
M itaan «■ lUt poiBt (Saint llartia't ediaon. ii. j». SeS).
' * n* peeadiBr iatetcat wUil Ite aatlor (Satat Maiti^ S. f. SM)
takea ia Oa eaigia of tbe Ebn is noea aa tot oplaaed ly a* «ar
agaiait tbeaa «Aitb caOed tka caapoa* fv-->— - IL aKar&<*a <ka
East in tie rear «S7. Ia attar nmmta the writer feyhfa fta —at
oamidete indiSnM^ aa4 a«a jgimaian vitt ngard to tie aMe af
a&in ia tie Wait.
* a. Laagam,a. a. * CL la^ae, (^
1 755. shortly after the eompletiaa of m
improved editioa of his Clumk Hularf.
Yta MaakeiBi'a pSaoe aa aa rnclraaitii |1 hataiia, an «>fw
HinoBT, ToL V. p. 7SS. b fUa JuiailMiiat af Etota^ m
additiiai to the rartfarfawaw aaaat ha aniiiiillj ■lalii^iil UaZk
BOnu Orfrtaaaraai aatfe OaaitaatfaaBB J^aaaa Aauaarivii
r-") —"^^ — -jilt mill jam "l<aa|aafwa<1 rhiaTTiliiMi.
kaa indcpeBdeat tfcaa La Oar^ laaa f^paisaa Chaa BeaaaalRV tiba
hiatoriaa Xiaheia ia faSi, ritiMal. »»— — * aal Bodoate.' *»«■
rrwrtfal wiiliagi^ ehiiailwiaed I17 liaiaiai, aad oaad aeas^
iai^ide dyOafieaea aa JT. r. be aafat (ITMIi, aad iiiiiiiBlim
oTlCoi^ a74I)aad1ha tBwX^adaata'tbastkjraTSS). U^
senaana {EfOifi teit») rrMj^rriWu tUtptmtm ia Aoara, aad a
iiiiiliiij iifiljlli aliii^ ja^ifiiii lh<n>iaili<» hihljl aa |i iiiiiili ■! tt
Oe Gcnaaa Soeieto'. Tktc a» twa Va^iA tcdhm at Ika far'
Utit», Qat dL TtaAaa^ pnMiAwi ia ifc^aad that aT Mariadc
(1832), which ia amda aaoR esaaeL lh« latter waa tsriaad aad
re-edited by Bead ia IMS. AaE^QAtnadailaea«rihaik.&fcu
Chriatianffrwai, begfim ia U13 hj Tidal, wia easaHefead sdI adifee^
by Unrdodc in IB9I.
MOSQUE {JiaiC, or oore faOj Ua^U Jdmi. the phec
of eongregatkmal prayer). Owing to the almoet eoaqileta
ahsenoe d ritual in the lf<»iJ<»»i» woniiqs, the aMawa^ at
least in its eariier foiau^ is ome of the aoplsst of aO i»
ligiooB bmldii^i, — its nomal aneogan^ heing aa open
oomt {SaJkm) samnmded bj s eorered doister {limSm), id
theoeBtreof vhidi is a astern for Ae ahfadiaBS leqfBBtr
before prsTer (JfUs'a) ;* the side of Ae nosqpM wUch it
towards lleccs isonmpiffd tijaroofed binUiBg(Jliiir£rB),
or place leaiaied for pnyei; aonetJBies seieeued off faga
the oonil^ hot freqnentljr quite open toa'sids it. la &e
ocBtre of this mnrtnary is » nidie {UikrA or KMa)
(having the direction of Meeea; aad hf the tide of the
nidie is a ioftjpalpit (JAaabor). Ia fnot of the pal^ is
a raised ^atfonn {fiaUxi) &aas wUch certain rThirfifics
are r'i^t'A^ and near it one or Bote seats aad betetna
ootnhiiMid faaavhidt chiqitecsaf the Eonaaie icad to
the pgople.
Minareto {lUMU, ast^ lUJkama) woe aot h«lt
dming the first half-eentaiy after the Flig^ hat now as
a rale no laaaqiM is without at least aba. IVaaithea|iper
gslleiy of this the JUocdbiJaM aanoanees to the fudrfial
the times for pcayei; — fire times dming ^ day, and twice
at night. Blind men are geaerslljr aefeeted far this offes,
so that dief may not oreriook the neigbbaming toosea.
Moat moegpes fasTe eadowed'propertjr, -wiaA is admi-
nittered hj a warden (S4zui), who also appasatstbe imims
aad other i^ciala. The larger masques have two imims :
one is called (in Aiahia aad E^n>t) the KhttSk, and he
pleaches the sermon on Fiidsjs (the Ifosiem fiahhath) ;
the other, the BiStib, reads Oe Kona, aad ledta- Ae five
daOj fojaa, standing dose to the Jl^rA, aad Iea£ng
the congr^aliaa, 1^ repeat the pnfcn wi& Use, aad
doselj follow hb postarea. the imtms do not fotm a
priestly sect; Aey geaerally have other «WTiipatioa^ sach
as tfaAitng in a ackool or ^"f^z a Aap, and may at any
tia>e be dianissed by the aaiJea, ia wUdh case they hies
the title of imiaa. Dooriceepecs aad attendaata to sweep
the floor, trim the laaqi^ and peiftam other fnisl offeei^
are attadied to eadi mosqae^ in mimben vaiyiag aeeotdi^g
to its oie aad cadowmeat. Iftwlias wasaea, as a lok^ aM
expected to s^thctr pcqren at hoBM^ but ia some few
monqnes diey are admitted to one part spedaT.y sereeacd
off tor them. This is Ae ease ia the mos^te of EStta
Zaiaab in Cairo. In the Ahai moaqne at Jenimlem there
is a latticed faaleaay for Ae wtomea, wtecaa me withoat
being viable to the male wonhippen below.
The greatest poasifale ^dwidnnr bott of material aad
mwimsmhy is often lavished oa Os baildiag aad its
* fa ■iiiinaia rnnaiiiiliii bj Tiala ai atbaa 1
aaet avaaa^ watca ia |aawidea fraa a aaaaad laak wiA fl^awff jrt^
caBad a imma/ifft aflar tta aeet who 1 ' '
aaaaaaS ta waak ia a alagaaat taafc.
864
MOSQUE,
3ttinf;5. The ivliolo outside is frequently decorated with
the luoat elaborate surface-carving in stone or marble, — the
(lavement of the richest marbles, inlaid in intricate patterns,
the walls panelled in a similar way, or decorated with
the most minute mosaics of glass, mother-of-pearl, agates
and other costly stones. The central niche and the pulpit
•ire of special magnificence ; and, if the latter is of wood,
it is often covered with delicate ivory carvings, and inlay
of pearl and ebony. Very beautiful surface-ornament,
executed in hard stucco, and enriched with gold and colours,
Ls used to decorate arches, wall surfaces, and the penden-
tives of domes, wliich latter generally have the so-caUed
"stalactite" form of ornament — one of great beauty and
complexity. The woodwork of doors, screens, and ceilings
is frequently very gorgeous with carving, inlay, and ela-
borate painting ; the whole of the doora outside are often
covered with very delicate pierced and embossed work in
bronze, or more rarely iron. Tiho magnificent tiles from
Persia, Damascus, and Rhodes, enamelled in brilliant blue,
green, and red, on a white ground, are often used to cover
the walls. Traceried windows in pierced marble or stucco
work often occur ; these are filled with brilliant coloured
glass, -always in very small pieces, forming a transparent
mosaic of jewel-like richness.' Lamps of enamelled glass,
or of bronze inlaid with silver, were once common, but are
now rapidly disappearing.
Some mosques, especially me Karubin mosque at Fez in
Morocco, possess a collection of magnificent illuminated
SISS., chiefly copies of the Koran and other religious boolcs;
ip the large collection at Fez, MSS. of Aristotle's Natural
Histori/, with the works of Averroes and other commenta-
•ors, exist in considerable number ; some few of the MSS.
are as early as the 10th century.
Plans of Mosques. — Considerable diversities exist in the
plan and arrangement of mosques in various countries, either
because the iloslem conquerors adopted to some extent
the existing buildings and architecture of the conquered
people, or on account of the new mosque being built on a
site already cramped by surrounding buildings. The first
of these causes influenced to some extent the mosques of
India, and to a much greater extent those of European
Turkey. The second cause, the cramped site, especially
in Cairo, created a special typo of plan. Nevertheless,
when free from such distui'bing influences, there is one
normal plan adopted, tt least in early times, by the Mos-
lems in all countries — from India to Cordova, and from
northern Syria to Egypt.'' This normal plan is a very
simple one, and is the natural product of a country like
Arabia, unskilled in architecture, where land was worth
but little, and timber very scarce. (See fig. 1.) ■
Though not the earliest, the great mosque of Cordova is the most
magniticent, and in the main the best preserved, of this typical
form.' It was begun in 7S4-5 by the caliph 'Abd al-Kahman I.
(Abderame) and completed by his sou Hisham in 793-4 ; though it
was afterwards enlarged, and then to some extent injured by addi-
tions^the work of the Christians, who made it into a cathedral —
yet it still remains but little altered, except by the loss of its mag-
nificent carved and inlaid wood celling and sumptuous Mimbar.
It consists (omitting recent additions) of hvo main parts, a largo
cloistered open court, with at one side a covered building for
prayer. In one respect only it dilfers from the usual plan : the
open court is generally much larger than the roofed space, whereas
at Cordova it is smaller. For the sake of brevity this arrange-
ment \vill, in the rest of the article, bo referred to as the *' normal
)ilan.*' In spite of neglect and alterations this mosque is still one
of the most imposing buildinga in the world. The long ranges of
« See Coste, ArdiiUcture .^rai«/h837-39 ; Bourgoin, Les Arts
Arabes, 1863; Prisse d'Avennes, Art Arabt, 1874-80; ^ai Tcxier,
VArminie et la Perse, 1842-62. ' ■
• The great mosque of Mecca (y.e.) is nnlqne in plan. ' For an
•cconnt of the mosque of Medina, sec Medina.
' CoBtreraa, Arte Arabi en Espalta, 1875 ; AcademTi, 19th Novcm-
l»r 1881, " Mosque of Cordoba," by J. H. MiddUton yMon. Aniui. dt
Xifana \ and Prtngey, ilotquic dt Cordoiu,/
s.U\ez, nineteen from cast to west and thirty-ono from north to
south — on their liiarble columns the spoils of many a Greek and
Roman temple — secni to stretch almost endlessly in every direction,
and each range of pillars appears to lose itself in the gloom of
distance, so that from no point can any idea be formed of what is
the real size of the whole building. The side towards the court
was quite open, and all over the court orange-trees were planted
at regular intervals, continuing the lines of the columns within,"
and set at the same distances apart ; so that aisles of orange-trees
in long ranges covered the open space, just as the marble columns
did within. No words can describe tho jewel-like splendour of tha
mosaics in the sanctuary, which in compUcated Arabesque patterns,
mixed with elaborate Cufic inscnptions, cover tha walls and even ths
arches, which cross and recross each ciher in tho most fanciful and
daring way, forming a sort of aisle round three sides of the sanctuary.
There is documentary evidence to show that these glass mosaics,
though of thoroujjhly Oriental design, are, like those in the mosques
of Jerusalem and Damascus, the work of Chiistian aitists froia
Byzantium.
The most important early mosques were all built on this normal
plan, with but very slight variations. Tho following are some of
the finest examples of this type : —
Mosque of 'Amr, Old Cairo, begun in 642 A-D., but much en-
larged at the end of the 7th century, and afterwards partly
rebuilt (see fig. 1).
Mosque of Sidi-'O.kba at Kairawan in Tunis, latter part of 7th
century.
Mosque of Sidi-'Okba near Biikra in Algeria, about 684.
Mosque of Edris at Fez in Morocco, end of 8th century.
Great mosque of Damascus, 708.
Great mosque of Cordova, 784-794 (described above).
Mosque of Ibn Tulun, Cairo, 879.'
Mosque of Al-Azhar, Cairo, begun about 970.
Great mosque at Old Delhi, 1196-1235-
Tho first of these, the mosque of 'Amr (see Costo, Arehilectun
ii ii -i § S -i 11 H it ij M ;:
Fio. 1.— Plan of Mosque of 'Amr, Old Cairo.
1. S^bla. 2. MIrabar. 3. Tomb of 'Amr. 4. Dakki. 6. Fountain for Ablu-
tion. ' 6, 0. Rooms btult lator. 7. Mlnarot. 6. Latrines.
yfralx), is now in a partly ruined condition. Its east wall probably
still retains some of the ori^nal work of 'Amr, who in 642
built a small mosque on the site of the present ono. But little
remains except its fine antique marble columns to tell of its
former splendour in mosaic, stucco reliefs enriched with painting,
and magnificent inlaid wood ceilings and screens. According to
Makr'i, it once contained 1290 MSS. of the Koran, and was
lighu.- by 18,000 lamps. In genera! effect, like all mosques of
tliis simplo and extensive plan, it is very stately, from th^Vast
size of its area, and its great number of closely-ranked columns
and arches, the Utter being of many fovios — pointed, s«micircula^
MOSQUE
865
and horse-»ho«. Kig. 1 gives its plan as a good typical specimen
of tUia normal type of mosque.
The mosque at KairawAn, Tunis, said to have been founded by
•Okba (see supra, -p. 567), follows the normal plan, with 439 fine
antique marble columns, horse-shoe arches, some pointed and others
round, and flat ceiling of dark wood, once magnificently painted.
Its sanctuary is ten aisles deep by seventeen wide. In the centre of
the court is a marble fountain over the sacred well, said to communi-
cate with the spring Zemzem at Mecca. Its minaret, a rather later
addition, is very massive and stately ; it is square, in three stories,
each battlemented, the walls battering considerably. The sanctuary
is domed, and the Mihr&b is decorated with magnificent tiles.
Adjoining the sanctuary is a small room for a library.
The other great mosque of Sidi-'Olcba, built soon after his death
in 682, and containing his tomb, is in Algeria near Biskra ; it
much resembles the Kairawan mosque, but is less splendid, some
of the columns being' not of marble but of .baked clay decorated
with painting.
The great mosque of Fez, about the same date, is also very large
and magnificent, with Mimbar and Mihrdb richly ornamented with
minute mosaics ; it has also a fine inlaid and painted wood ceiling,
and some elaboratcIy-carved doors. It still possesses a fine library.
(See Amici, Journey to Fez, 1878.)
The great mosque of Damascus was built on the site of a
Christian basilica, erected by Theodosiua in 395-408. From 636,
when the Arabs conquered Damascus, until 708 this basilica
was used jointly both by the Christians and the Moslems. The
basilica was then pulled down, and the present mosque built by
the caliph Walid. It has the normal plan, and is 608 feet by 320
feet. Its sanctuary is only three aisles deep ; it has a central
dome on the south or Mecca side, and on the east and west a large
porch. Samhiidi records that one of the conditions of peace con-
claded between the Byzantine emperor and WaUd was that the
emperor should fuTHish a certain number of workers in mosaic
for the decoration of the mosques at Mecca, Medina, Jerusalem;
and Damascus.
The mosque of Ahmed Ibn Ttilun, in Cairo, completed in 879,
has the normal plan, with the exceptional addition of an outer
court, or wide passage, nmning round three sides of the rectangle, —
probably to cut it off completely from the noise of the surrounding
atreeti. It is built of brick, coated with delicate reliefs in stucco,
once enriched with painting. The Mihrdb has beautiful mosaics,
and the Mimbar is a marvel of delicate carving and inlay. The
fillars and arches are of brick enriched with elaborate stucco-work.
t has a very remarkable minaret on the west side, with a spiral
external staircase. The architect was a Copt, an Egyptian Chris-
tian. It is perhaps the earliest important building in which the
pointed arch is largely used.
The mosque Al-Azhar, "The Splendid," was built in the centre
of New Cairo about 970 and, thongh frequently restored, has
in the main been little altered. It is on the normal plan, with
ranges of pointed and slightly horse-shoe arches, supported on more
than 400 fine antique columns of marble and pbrphyry, chiefly from
Roman buildings. Among its later decorations are magnificent
wall-coverings of the most beautiful Persian tiles. It has a special
interest in being the chief university of the Moslem world, con-
taining some thousands of students {mujdvnrin), for whom certain
parts of the mosque {Siwdk) are screened ofi*, according to the
country from which they come. Thus special parts are reserved
for natives of the various provinces of Egypt, of Morocco, Syria,
Arabia, India, Turkey, &c. Each student can, if he is too poor
to hire lodgings, live, eat, and sleep in the mosque. Each has
a large chest in which to keep his clothes and books ; these are
piled against the walla to a height of seven or eight feet. The
students pay no fees, but the richer ones give presents to the
lecturers, who ait on the matting in various parts of the sanctuary
or cloister, while the students sit round each lecturer in a circle.
The usual course of study lasts for three years, I^hough some
students remain for much longer. The chief of the lecturers, called
the Sheikh aUAshar, receives about £100 a year, the others little
or nothing, as regular pay. The Koran, sacred and secular law,
logic, poetry, and arithmetic, with some medicine and geography,
are the chief subjects of study.
Of mosques which are not built on the normal plan the earliest
and most important are the two in the Hardm al-Sherlf (High
Sanctuary) at Jerusalem (see vol. xiii. p. 642).
The Kubbet al-Sakhra (Dome of the Rock), popularly, butwrongly,
called the "Mosqne of Omar," is not, strictly speaking, a mosque
at all. It belongs rather to the class of " shrines, — ^generally small
square, circular, or octagonal buildings erected over some sacred
spot or tomb. It is a very beautiful building, with high central
dome, and double ambulatory round it, — the outer wall being octa-
fonal, and the dome, with the pillars that carry it, circular in plan,
t is decorated in a very sumptuous way by inlay of rich marbles
and very splendid glass mosaics. The outer wall and most of the
internal mosaics are later than the dome itself. Its windows of
motaiciike stained glass are very beautiful, and are almost the only
10— ;i;j
Moslem example of the use of lead " cames," instead of the bits of
glass being fitted into marble or stucco tracery ; this, as well as the
glass waU-mosaics, was probably the work of Bylantine artificers.'
The mosque within the same enclosure, called Al-Aksd, is entirely
roofed, with many aisle.'i and columns, having no open court, quite
unlike the usual arrangement of a mosque.
The finest and largest group of mosques is at Cairo. Many of
them are very complicated buildings, with no resemblance to tlie
normal plan before described. In some cases a hospital, a school, a
court of justice, a monastery, or very frequently a tomb, forms part
of the building, and causes considerable modifications in its plan.
The finest of these is the mosque of the sultan Hasan, built
between 1350 and 1359 (fig. 2), a good specimen of a mosque
built in a crowded site
with a wing for a tomb.
In plan it is cruciform,
the central part being
open to the sky ; the
eastern arm of the cross
is the sanctuary, and
farther east is the stately
domed tomb of the sul-
tan himself. All four
arms of the cross are
vaulted in stone with a
plain waggon vault. Its
magnificententiance en
the north; with an en-
ormously high arch, de-
corated with stalactite
reliefs in stone, is set
somewhat askew to fol-
low the line of the old
street. It has two mi-
narets, one of great
height and grandeur.
The MuristAn Kalaun
is a combination of
hospital, tomb, and
mosque, — an enormous
buildingcovering a very
large area. It was built
by Sultan Kalaun at the
beginning of the 14th
century; his tomb, built
1320, which forms part
of this great building, is f'"- '•— Plsn "t Mraq„e of Saltan Hasao, Cairo,
a massive square edifice l, 2. Main entrance. S. Court open to sky.
with a very grand and *. S- Fountains. 6, 6. North and south vaulted
well-desianed octaconal '™''»«Pf' (the dotted lines show the curve of the
^.Trn» I?» „.11 \n3li„. ^aolt . 8, 6. D.kka. 10. Sanctuary. 11. Mimbar.
dome. Its waU-mosaics 12. Klbla. 13. Door to tomb. 14. Domed tomb-
in pearl and precious chamber. 15. Tomb within screen. 18. Eibla.
stones are unusually ^^' ^'^- Minarets. 18, IS, 20. Various entrances to
-n»/»i;A....»4- 17 -. mosque. 21. Small rooms connected with service
magnificent. Even a „, ^e mosque, sa. Sultan's private witnmM!^
bare list of the mosques
of Cairo would occupy a large space ; they are over four hundred
in number, and are mostly remarlcable for some beauty in design
or richness in their ornament and materiaL
The mosque of Ibrahim Agha should specially be noted for tho
splendid Persian tiles which cover the east wall of its sanctuary ;
these are of the end of tho 16th century, and are unrivalled in
beauty both of drawing and colour. The tiles are 9 inches square,
and work into large designs with very graceful sweeping curves of
foliage, drawn with the greatest skill, and painted in the most
brilliant yet harmonious colours — perfect masterpieces of coloured
detoration. See Mubal Decobation.
The so-called '* Tombs of the Caliphs," really tomb-mosques of
Egyptian sultans, are a large group of very fine buildings, less tiian
a mile nutsido the walls of Cairo. Tho largest is that of Sultan
Barkiik, with a superb dome and two stately minarets. In addi-
tion to an extensive open court, it has on each side of the sanctuary
a magnificent tomb-chamber containing the bodies of the sultan
himself, who died in 1399, and various members of his family.
The most beautiful and graceful of all these mosques is that which
contains the tomb of Sultan K&it-Bey, who died in 14,96 ; its
dome is entirely covered externally with beautiful and delicate
reliefs carved in stone. Its minaret is a masterpiece of invention
and extreme graca of outline, combined with the richest and moat
exquisite det^ ; like most of the Cairo mosques, its exterior ia
ornamented by bands of red stone alternating with the yellow
Mokattam limestone. Inside, marble inlaid pavements and mosaic
on the walls, with decorations in painted stucco and wood carved
and inlaid give extreme splendour to the building. Fig. 3 gtvee
its plan as a typical example of the combined moeqne and tomb,
— the lattar the more important The mosque in«id«,th» w«ll» of
» fiee Do Vogue, Xemnk is lirutaiem. 1864 ; Teider. -itU IHunn, U»
866
M O S — M O S
Cairo, built by tbe same sultau, is also very beautiful, and re-
markable for its carvings and ^
mosaics.
It should be observed that the
magnificent mosques of Egypt,
as of other countries, owe little
or nothing to the native archi-
tectural taientof the Arabs them-
selves. Their own buildings at
the time of the Prophet were of
the simplest and rudest descrip-
tion, but they were always ready
to make use of the architectural
skill and constructive power of
thepeople they conquered.
The earlier buildings of Egypt
are mainly the product of Coptic
and Byzantine skill, while rather
later the art of Peraa, both in its
general designs and details of
workmanship, exercised a para-
mount influence over the whole
Moslem world. Another influ-
ence must not be forgotten, that
of French and English Gothic, __
produced by the buildings erected pj^ 3 _jj^5q^,^.t^j„b of g^^jta^ giit.
by the crusaders dunng their oc- Bey, Cairo.
cupation of Palestine. One of the , jj^j^ entrance. 2. Lobby and cIs-
Cairo mosques, that of Kalaun, terns for ablution. 3. Gr^t minaret,
possesses a fine arched doorway, 4. Kibla. fi. Mimbar. 6. Saltan's tomb-
Uken from a Christian church f^-^^^ 7. The tomb within a screen,
at Acre— a fine specimen of Early
English work, which would not be out of place in Salisbury Cathe-
dral. Moslem translations of the clustered jamb-shafts and deep
arch-mouldings of this style often occur.
The rest of northern Africa contains many mosques of great size
and splendour ; among these the most important, in addition- to those
already mentioned as having the normal plan, are— (1) the mosque-
tomb of'Abdallahb. Wadib in Kairawan, Tunis, a very large build-
ing, cont.iining several courts and cloisters, dating from the saroe
early period as the other gi*eat mosque in Kairawan ; its minaret is
covered outside with fine blue and green tiles ; (2) the gi-eat mosqua
of Algiers, 10th «entury ; and (3) that ef Tlemcen, in the extreme
west of Algeria, built in the middle of the 12th century ; this has a
very splendid pavement, partly composed of Algerian onyx, and a
beautiful bronze chandelier, 8 feet in diameter, given by Sultan
Yarmorak, 12 48-83.
In Spain, at Zahra near Cordova, was one of the grandest of
the early mosques, finished in 911 : but nothing of it now exists.
Several churches in Spain were originally built as mosques, such as
S. Cristo do la Luz at Toledo, a small, nearly square building,
roofed by dome-like vaulting on marble pillars.
In Persia but little now remains of the magnificent early niosques,
built with such splendour, especially during the reign of Hariin al-
lUshid. At Erzeroum there is a fine mosque, combined with tomb
and hospital, almost Early Gothic in style, dating from the 13th
century.' At Tabriz there is another church-like mosque, evidently
the work of Byzantine builders ; according to Texier, this belongs to the
16th century, but it is probably two or three hundred years earlier.
The mosque of Houen, near Cresarea in Cilioia, is a fine largo
rectangular building, covered with low domes on square piers. It
dates from the second half of the 12th century.
At Tchekirghe near Broussa is a very remarkable mosque — that
of Murad I., built in the 13th century, almost in the style of con-
temporary Italian Gothic. Its main facade bears an e.\traordinary
resemblance to one of the earlier Sienese palaces.
The later capital of Persia— Ispahan — became the centre of the
highest development of the Persian arts under Shah 'Abbas I.,
1585-1629 ; to this period belongs the splendid mosque called
Ma^id Shah, a strangely-planned Duilding of great size, enriched
in the most sumptuous way, inside and out, by waU-coverings of
the finest Persian enamellod tiles. The mosque of Sultan Hosein,
built as late as 1730, preserves much of the old beauty of design
and decoration.
India is especially rich in mosques of great size and beauty. The
earlier ones are muck influenced by the still older Hindu architec-
ture, and some of the larger mosques are built of materials from
the old Jain temples. It is recorded that twenty-seven Hindu
temples wore destroyed to build the great mosque in Old Delhi,
erected 1196 to 1235, which presents a curious mixture of the
semi - barbarous Hindu carved work with the more refined and
graceful decoration of the Moslem builders. This great mosque is
on the normal plan, as is the 13th century mosque at Ajmir, also
' See Texier. LArirUnit cl la Peril, 1842-52 ; Coste, Monuments
Modtrna de U>. Perse, 1867 ; Flandin and Costo, Voyage m Perse,
184S*e4.
built on the ruins of & Hindu temple. A whole Tolome would not
suffice to describe the magnificent mosques of India, euch aa those
at Ahmedabad, Mandu, Maldah, Bijapur, Fathipur, and countless
others. Tho introduction in thfl 17th «entury of Florentine marble
and mosaic workers produced a new and very splendid style of
building, of which the "pearl mosque" and the Taj Mehal at Agra
are the linest specimens.
At Srinagar in Kashmir there is a large and very remarkable
mosque of the normal plan, constructed entirely of wood logs, with
numerous pillars of deodar pine ; it was built by Shah Hamadan,
and is an extremely picturesque building. (See Cole, Ancient Build-
ings in. Kashmir, 1869.)
In Turkey the mosques are either old Christian basilicas, such
as S. Sophia and S. Saviour's at Constantinople, and tho numerous
fine early churches of Thessalonica and Trebizond, or else are mostly
copies, more or less accurate, of Justinian's splendid church of S.
Sophia, a building which seems to have been enthusiastically ad-
mired and appreciated by the Ottoman conquerors. The mosque of
Solaiman the M.agnificent, 1550-1555, is the finest of these Turkish
reproductions of S. Sophia. Another, rather less close a copy, ia
the mosque of Sultan Ahmed, 1608. None of this latter class are
of course earlier than the middle of the 16th century.'
In the present century Mosfem art has produced but little of
architectural importance The great mosque of Mohammed Ali, on
the citadel of Cairo, is the work of a German architect, and thoagh
built of rich materials is of small artistic value or interest ; it ia a
large but feebly designed building of the S. Sophia type. Unfor-
tunately European influence seems now to be rapidly destroying
the feeling for true art that still survives among Moslem nations.
liUrature. — In addition to works referred to above see Monumfnloi Arguitee-
(■jnicos de Esj^ana, 1859-S3 ; Murphy, Arabian Antiquities of Spain, 1813 ; Owen
Jones, AthAmbra, 18-12; Antiguedades Arahes de Espana, 1870 ; Hay's Views in
Cairo, 1840 ; Roberts, Boly Land, Egypt, &c., 18i2-9 ; Hessemer, ArabischM
Bau-i^erzierungen, 1853; Castellani, Architettnra OrientaU; Launay and Mon-
tani, Architecture Ottomane, 1873 ; Salzenberg, Alt-Chrislliehe Bnudenkmait
ron ConBtantlnopei, 1854; Lewis, Iltvstratioits of Ccnstantinopte, 1837; Chardio,
Voyage en Perar, 1735; FeTgaBsosi, Architecture of lndia,&c., 1876; Colo. Ancient
Delhi. (J. H. M.)
MOSQUITO (.sometimes written " Mo-squita "), a Spanish
word signifying " little fly," is a name popularly applied
to certain annoying dipterous insects, and, strictly speaking,
it should probably be used only for species of Ciilicidac
(and for the genua Culex in particular), for which "gnat"
is the English synonym ; but in many countries it is by,
almost common consent applied to all small dipterous in-
sects that suck human blood, and therefore includes what
we know as "sand -flies," "midges," dx., of the genera
Ceratopogim, Simulium, and others. By Englishmen a
distinction is often falsely drawn between " mosquito "
and "gnat," the former being suppesed to represent an
insect natiye chiefly of hot climates, whereas the latter
is their own too-well-knowu pest. In effect the terms are
really synonymous, and any ac'jual difference can only be
specific. In very hot seasons we not uncommonly hear
alarming reports of mosquitoes having made their appear-
ance in London and elsewhere in the British Isles, and
means whereby they were imported are often suggested, —
the real facts of the case being that extra heat may render
the native species more annoying, or that it causes a bodily
condition in which their bites are more severely felt.*
The "mosquitoes" of high northern latitudes may be
species both of Cnlex and Simiilium.
Accounts of tho numbers of these insects in tropical
countries and in high latitudes, and of their irritating
attacks, are to be met with — seldom exaggerated — in most
books of travel. Even in Britain the annoyance caused
by gnats is very great, and in marshy districts often unen-
durable, especially to new-comers, for it seems probable that
the insects really attack a visitor more furiously than they
do the natives of the district, but, on the other hand, the
latter may bo more indifferent to their assaults. In some
subjects even the "piping" by which a hungry gnat
announces its presence has most distressiiig effects. In
" Texier and PuUau, Byzantine Churches, 1864 ; Pulgher, Jiglisu
de Constantinople, 1882.
' A few years ago a London hotel, popular with Araeric'.n nsitora,
was said to harbour mosquitoes, which some of the visitors had brought
with them from the Southern States. An examinatiou revealed the fac4
that the cistern was uncovered and exposed, and was the breeding-place
for hosts of gnatt.
M O S — AI O S
867
Ugh latitudes they are driven off hj anointing the body
with fish-oil ; and in hot climatea " mosquito curtains " are
part of the ordinary bed-furniture. It is only the female
that bites ; and, as it is but a very small proportion of them
that can ever taste human blood or that of any warm-blooded
animal, blood would not appear to be essential to their ^1-
fare. It has been suggested that warm blood may have
an influence on the ova, but it cannot be supposed that
the eggs of those multitudes of individuab that never get a
chance to taste blood are necessarily infertile ; everything
tends to prove the opposite.
Of late mosquitoes have been accused of playing a
hitherto unsuspected part in the dissemination of certain
entozoic diseases. According to the researches of Drs
Manson and Cobbold and others, it appears certain that
the insects, in sucking the blood of persons who are hosts
of the entozoon known as Filaria sanguis-hominis, take
these parasites into their own system, and it is believed
that they afterwards (by their death and otherwise) con-
taminate drinking water with them, and thus convey the
entozoa into the blood of persons previously unaffected.
Mosquitoes are aqoatic in their early stages. The
no. 1.— Moxjolto (C«I«). A, Mtnral tiie ; B, enlirged. (Atttr Curtis.)
female deposits her eggs in boat-shaped masses on the
surface of the water. The larvae are very active, and have
a peculiar jerking mo- ^
tion ; the last segment
is furnished with a
respiratory apparatus,
the form of which pro-
bably varies according
to the species, but it
is usually a long tube,
the extremity of which
can be exposed to the
external air. Thepup^e
are also active (contrary to the condition in most dipterous
pupae), and are odd-looking creatures owing to the great
development of the thoracic region ; the respiratory ap-
paratus is in the thorax in this state, the extremity of the
body having two swimming-plates ; the pupae do not eat,
but their activity is very great.
No notice of tlie mosquito or gnat ivouid be complete without an
explanation of tho mouth-parts by%hich it is enabled to cause
such extreme irritation. When these parts are closed one upon
the other the whole looks like a long proboscis ; but in reality this
consists of seven distinct slender pieces separated to the base, viz.
tho labium, two maxill.-e, hvo mandibles, tho lingua, and the
labrum. The nomenclature of the mouth-parts varies with different
•othors. O. Dimmock (Anatomy of the Mouth-parts aiui of the
SuckUy-apparalus of some Dijitera), tho latest investigator of this
complex apparatus, states that the labium has for function, for tho
most part, tho protection of the fine setse which form the true
piercing organ of Ciilcx. In the female .of Ciilcx the protective
sheath is formed by the labium alone. When the mosquito has
found a place which suits it for piercing— for it often tiics different
places on our skin before deciding on one— it plants its labellx
tirmly unon the spot, and a moment later tho labium is seen to be
flexing backwards in its middle ; the seta, fi'mly grouped together,
remain straight and enter tho skin. MThen the seta have entered
to nearly their full length, the labium is bent double beneath the
body of the insect. When the mosquito wishes to withdraw the
seta it probably first withdraws the two barbed maiiUa! beyond
the other setse, that is, so that their barbs or papillae will be kept
out of action by the mandibles and hypopharynx ; then it readily
withdraws the sets, perhaps aiding their withdrawal by the musclu
mgiV,.-;;..i-.ii.'!;'fin.T.
Pio. 3.— Mouth-parts, &c., of remade Cultx (after Dimmock). a, antennc'
e, olypeus ; ft, hypopharynx ; Ir-e, labrum - epipharynx ; t, labium • ml
mandibles ; nu, nmxillse (with the tip of one of them eiilarged). '
of the labium, for during the process of extracting tho seta from
the skin, while they are slowly sinking back into the groove upon
the upper side of tho straightening labium, the mosquito keeps
the labellse pressed firmly upon the skin. The withdrawal of
blood is effected by means of a pumping apparatus at the base
of the mouth - parts. As no investigator appears to have been
able to detect a poison gland, it has been considered that the irri-
tation caused by the bite of a mosquito was solelyof mechanical
origin ; but the extreme irritation and its duration have not caused
this idea to be commonly accepted. Dimmock avows his belief
that there is use made of a poisonous saliva. In the male of Culex
the mouth -parts vary considerably from those of ttie female, a
conspicuous point of difference being that in this se- the mandibles
are absent, and the maxilli£ are not barbed.
About 35 species of Culex (mosquito or gnat) have oeen described
as inhabiting Europe, and about 130 from the rest of the world,
but their differentiation is involved in great difficulty and uncer-
tainty, and it is probable that the number of true species may bo
very much less. A species from Cuba has received the name Culex
■nwsquito ; but there is not one species that specially deserves tho
name more than another fi-om a popular point of view, nor from a
scientific point of view is there any difference between a mosquito
and a gnat.
MOSQUITO COAST. See Nicaeagua.
MOSSES, or Musci, one of the two divisions of the
botanical class Miisciness, which includes also the Liver-
worts or Hepaticse. See MuscinEjE.
MOSSLEY, a manufacturing town of Lancashire,
England, is situated on the London and Norti-Western
Railway and on the Huddersfield canal, near the west bank
of the Tame, which here separates Lancashire from
Cheshire, 3 miles north-east of Ashton-under-Lyne, and 10
east-north-east of Manchester. The houses are for the
most part built of stone. To supersede the old church of St
George, erected in 1757, a new btiilding was begun in 1881.
A mechanics' institute was erected in 1 858. In the vicinity
of the town is an eminence called Hartshead Pike, on which
is a lofty circular tower surmounted by a spire rebuilt of
stone in 1758. Mossley has risen into importance since
the introduction of the cotton manufacture about fifty
years ago. A fair is held annually. The town was placed
under the Local Government Act in 1864, the district to
which its provisions extend including also part of Saddle-
worth in Yorkshire. The total population was in 1871
10,578, and 13,372 in 1881.
MOSTAK, the chief town of Herzegovina, is built on
both banks of the Narenta, about 35 miles from its mouth,
and 40 miles south-west of Seraievo (Bosna Serai), the
capital of Bosnia. Among the public / buildings are a
palace, two Greek churches, and forty mosques, in several
cases with Roman or Byzantine tracery in their windows.
The fine old bridge from which the town takes its name
868
M O S — M O S
{Most, Star, Old Bridge) is probably Roman. The town
has a good trado and manufactures excellent Damascus
swords ; and the grapes and wine of Mostar are celebrated
throughout tha south Slavonic countries. The population,
7300 in 1844. had increased to 10,848 by 1879.
Whether its ancient name waa Saloniana, Sarsenterum, or An-
dretium, there is little doubt that -Mostar, or, to use the older
Slavonic name, Vitriniteha, dates from the time of the Romans. It
was enlar^red in 1440 by Radivoi Gost, mayor of the palace to
Stephen, hrst duke of St Sava. Immediately on their conquest of
Herzegovina it was chosen by the Turks as their headquarters ; and
it afterwards tecame the capital of the independent government of
Ali Pasha and Stolac.
See Evans, Through Bosnia and fferzegovina, 1S76 ; Wilkinson's DalTnatia and
MonUneffTo, vol. li. (view and plan at pp. 69-60) ; and Calx de Baint Aymoor in
RiV. dts D. Moiwcs, February 18S3.
MOSUL, an important town in Mesopotamia, on the
right bank of the Tigris, in 36' 35' N. lat. and 43° 3' E. long.
In Mosul, as in Baghdad, only part of the space within
the walls is covered with buildings and the rest is occupied
by cemeteries ; even the solid limestone walls of the ancient
town are half in ruins, being serviceable only in the direc-
tion of the river, where they check inundations. Of the
town gates at present in use, five are on the south, two on
the west, two on the north, and the great bridge gate on the
east. Leaving Mosul by the last named, the traveller first
crosses a stone bridge, 167 feet long ; then a kind oi island
(140 feet), which is overflowed only in spring and summer
by the Tigris ; nest a stretch of the river which, at such
tunes as it is not fordable, is spanned by a bridge of boats,
the bridge proper covering only one-sixth of the full width
of the stream. During the season of low water excellent
vegetables, particularly water-melons, are grown upon the
islands and dry portions of the river-bed.
The interior of Mosul has an insignificant appearance, only a few
of the older buildings being left, amon^ which may be mentioned
the Great Mosque, with its leaning minaret, formerly a church
dedicated to St. Paul. The private houses are partly of brick and
partly of stone, the district furnishing an excellent and easily-
wrought building-stone resembling marble. Handsome well-buUt
halls {iw(.iis) may be seen in many houses ; the undergronnd
dwellings also, to'which the inhabitants retire during the day-time
in the hot months of summer, are well and solidly built. The
houses are high^ and during three or four months of the year the
inhabitants sleep on the flat roofs. The streets are for the most
part badly pa\ed and very narrow, a small square in the market-
place, overlooked by airy cofl"ee -booths, being almost the only open
space. The shops are few and poor. The industry, in comparison
■with former times, when the toi^ii had so considerable a manufac-
ture in " musl:ji *' as to give its name to that fabric, is V^ery unim-
portant ; trade also, which is almost exclusively in the hands of
native merchants, has fallen off greatly. Gall nuts^- gathered on
the neighbouring Kurdish mountain slopes, are mostly exported,
but are also made use of by native dyers ; and hides, wax, cotton,
and gum are sold. Very few Europeans live in Mosul, though the
market is abundantly supplied with European goods. The whole-
sale trade, conoucted by means of caravans, has greatly declined
from its former importance, owing not only to changes wMct have
been taking plate in commercial routes generally, but also to the
dangers of the roads near Mosul ; for to the north and east of the
town there are wild tribes of Kurds, some of whom continue to
assert their independence of the Osmanli rule, while the Yezidis,
a Kurdish tribe who have never yet accepted Islam, dwell in the
Siujar mountains, Upon a northern spur of which the town stands.
Serni-independent tribes of Bedouins al^io roam over the plains in
the immediate vicinity. The wild hordes of the Sharamar Bedouins
have often plundered or threatened the citizens. Mosul, therefore,
has a somewhat isolated position, and this perhaps is one reason
why Christians and Moslems have lived together on better terms
here than elsewhere.^ Both are animated by an active local patriot-
ism, and both honour the same patron saints, Jirjis (St George)
and Jonah ; the grave of the latter is pointed out on an artificial
mound on the left bank of the Tigris.
The language of the people of Mosul is a dialect of Arabic, partly
influenced by Kurdish and Syriac. The population is probably
25,000 to 30,000. It is stated that the town is divided into 32
quarters, of which one is Je^-ish and three are Christian, while the
rest are Moslem. The Moslems call themselves either Arabs or
iCurds, but the prevalent type, very different from the true Arabian
of Baghdad, proves the Aramsean origin of many of their number.
Of the Christians the community of the Chaldfeans, -i.e., those who
have gone over from Nestorianism to Catholicism, seems to be the
most important ; there are also Syrian Catholics and Jacobites.
Mosul has for several centuries been a centre of Catholic missionary
activity, the Dominicans especially, by the foundation of schools
and printing-offices, having made a marked impression upon an
intelligent and teachable population. There are very few Protest-
ants.
Mosul shares the severe alternations of temperature experienced
by Upper Mesopotamia (see Mesopotamia). The summer heat is
extreme, and in winter frost is not unknown. Nevertheless the
climate is considered healthy and agreeable ; copious rains fall in
general in winter. The drinking water is got from the muddy
Tigris. At the north-east comer of the town is a sulphur spring,
and 4 leagues to the south there is a hot sulphur spring (Hammam
'Ali), much frequented by invaUds.
Mosul probably occupies the site of a southern suburb of ancient
Nineveh (?.«.), but it is very doubtful whether the older name of
Mespila can be traced in the modem Al-Mausil (Arab., the place of
connexion); it is, however, certain that a to\vn with the Arabic name
Al-Mausil stood here at the time of the Moslem conquest (636 A.n.).
The town reached its greatest prosperity towards the beginning of
the decline of the caliphate, when it was for a time an independent
capital. The dynasty of the Hamdanids reigned in Mosul from 934,
but the town was conquered by the Syrian Okailids in 990. In the
11th century it belonged to the Seljuks, and in the 12th, under the
sway of the Atabeks, particularly of Zenki, it hhd a short period of
splendour. Saladin besieged it unsuccessfiilly in 1182. Among
the later rulers of Mosul the only conspicuous name is that of Lula,
in the first half of the 13th century. The town suffered severely
from the Mongols under Hulagu ; under Turkish rule it became the
capital of a small pashalik, bounded on the one side by the vilayet
of Diarbekr, on the other by that of Baghdad. The Persians
occupied Mosul for a short rime in 1623, until it was, soon after-
waros, recovered by Sultan Murad IV. It was visited by an earth-
quake in 1667, and was unsuccessfully besieged by the Persians imder
Nadir Shah in 1743. The governorship of the pashalik was long
hereditary in the originally Christian family of the 'Abd-al-Jalil,
until the Porte, during the course of the present century, succeeded
after a long and severe contest in establishing a more centralized
system of government.
Compared with what it was in the Middle Ages the present town
is mucn deteriorated, its decay having advanced steadily from the
beginning of the Turkish dominion.
See Rltter, Asien, voL vii A map of the town accompanies Cernik'a pap«r,
" Stadiencrpedition durcb die Ocbiete dc3 Euphrat ttnd Tigris," In Ergiuuuiige'
hflft No. 45 of PerarTTWim'j i/iri/ieiUnffen, 1970.
END OF VOUJME SDCEEENTH.
i
APPENDIX
AMERICAN REVISIONS AND ADDITIONS
ENCYCLOPAEDIA BRITANNICA
{NINTH EDITION.)
A DICTIONARY OF
ARTS, SCIENCES AND GENERAL LITERATURE
CHICAGO
R S. PEALE COMPANY
1891
0r K. & PojULf A:C«k.
MEMPHIS — MEREDITH
1071
the Confederate government was formed, he be-
came secretary of the treasury, and held this post
until 1864. After the civil war he lived in retire-
ment.
MEMPHIS, a post-village, the county-seat of
Scotland county, Mo., containing flour-mills.
MEMPHIS, a city of Tennessee, the commercial
!:n»tropolis of West Tennessee, and the most im-
portant commercial city l)etween St. Louis and New
Orleans. In addition to the facilities afforded by
the Mississippi River, on which it is situated, nu-
merous lines of railroads bring the products of a
large section of country to its wharves. The city is '
handsomely built on a bluflf overlooking the river.
It is one of the most extensive cotton markets of I
the country, the shipments of cotton amounting to ;
over 400,000 bales per annum. The principal man-
ufactures are iron, iron-goods, cotton-seed oil, lum-
ber, tobacco, farm-machinery, etc. Memphis has a
number of excellent public and private schools i
and seminaries. Population in 18^0,3.3,592; in 1890,
<>1.586. See Britannica, Vol. XV, pp. 847, 848. I
>LEXABRE.\, LfiGi Federico, M.^rqcis Vali.-
DoE.t, an Italian statesman, born at Chambery,
France, in 1S(W. He was professor of engineering
in the military academy at Turin. Afterwards he
served in the Italian ministry of war and of the
interior. In the war against Austria in 1859 he
was chief of staff, and fortified Bologna and other
cities, and conducted the siege of Gaeta. In 1861
he was made count and appointed minister of the
marine, and in 1867 he was minister of foreign
affairs. In 1875 he was created Marquis of Vall-
Dora, and in 1876 he served as ambassador to t
England. He is an accomplished mathematician
and engineer, and has published Le Genie Italien
dan> hi Compn.v.e 1S60-S1 0866).
MEXAGERIE, see Zoological Gabdes in these
Revisions and Additions.
MEXASHA, a city and railroad center of Winne-
bago county. Wis., eighteen miles north of Osh-
kosh. It has a number of manufactories. Popula-
tion, 4.-569.
MEXDE, the capital of the French department
of Lozere, on the Lot, in a valley surrounded by
high hills, sixty-six miles from Ximes. has a cathe-
dral, and manufactures serges and coarse cloths. I
Population. 6.740. See Britannica, Vol. XV, p. 31. j
MEXDELEEFF. Dmitri Ivaxovitch, a Russian j
chemist, born at Tobolsk, Feb, 7. 18.34, studied at
St. Petersburg, and, after having taught at Simfer-
opol, Odessa, and St. Petersburg, became professor
of chemistry in the University of St. Petersburg in i
1866. He has enriched every section of chemical ;
science, but is especially distinguished for his con-
tributions to physical chemistry and chemical phil-
osophv.
MEXDOTA, a city of La Salle county. 111., con-
taining an organ-factory and iron-foundry.
MEXIER. EjiiLE .IrsTix, a French manufacturer
.md writer, born at Paris, May, 18, 1826. died at
Xoisiel-sur-Marne, February 17, 1881. He estab-
lished at Xoisiel the celebrated chocolate factory,
chemical works at St. Denis, and a sugar manufac-
tory at Koye, besides a caoutchouc factory, and in
Xicaragua a cocoa plantation. A warm advocate
of free trade, he expounded his views in Economie
Rt.ray and in L'Avenir JEeonomiquf.
MEXIPPUS, a satirist who lived in the first half
of the 3rd century, b. c, was born a Phoenician
slave and became a cynic philosopher. His works
in Greek have perished, and he is known only
through the imitations of JIarcus Tarentins Varro.
See Britannica. Vol. XXIV, p. 93; Vol. IX, p. 655.
MEXOMIXEE, a city, the county-seat of Menom-
inee county, Mich., situated on Green Bay, at the
mouth of the Menominee River. Iron-mining,
marble-quarrying, and lumber-shipping are the
chief industries. Population in 1890, 10,606.
MEXOMOXIE, a city, the county-seat of Dunn
county. Wis., about twenty-five miles northwest of
Eau Claire. It is extensively engaged in tlie fur-
trade, has manufactories of iron, machinery, car-
riages, sash and blinds, and enjoys excellent edu-
cational facilities.
MEXZEL, Adolph, a German painter, lithograph-
er, illustrator, and engraver, born at Breslau, Dec.
8, 1815. He is best known for his drawings and oil-
paintings illustrative of the times of Frederick the
Great and William I., emperor — pictures charac-
terized by historical fidelity, strong realistic con-
ception, originality, and humor. His Adam and
J-^ie; Christ Among the Doctors, and Christ Expelling
the Moneti-changers, are also notable pictures.
MEPPEL, a town in the Netherlands province of
Drenth^, eighteen miles from ZwoUe. It has a trade
in butter and linen manufactures. Population,
8,418.
MERCADAXTE, Savekio {1797-18701. an Italian
composer, born at Altamura, June Ci, :'' 7, . ,,.,.. ?d
music at Naples, and began his career as a violin-
ist and flutist. In ISlS' he produce*' the first of
some sixty operas. From 1827 to l''ji he was in
Spain ; in 1S.S3 he was appointed musical director
in the cathedral at Xovara, and in 1840 of the con-
servatorv of music at Xaples. He died in that city
Dec. 17, 1870— blind since 1861.
3LERCED. a city, the county-seat of Merced
county, Cal., on the Central Pacific Railroad, 152
miles southeast of San Francisco.
MERCER, a post-borough, the county-seat of
Mercer county. Pa., sixty miles northwest" of Pitts-
burgh. Population, 2,134.
MERCER, Charles Fe.nto.v (1778-1856), an Amer-
ican soldier. In 1798 he was commissioned captain
in the L'nited States army, but subsequently prac-
ticed law in Fredericksburg, Va. Froni 1810 to 1817
he was a member of the legislature, and then until
1840 was a member of Congress. During the war of
1812 he was aide to the governor of Virginia, and in
command of the defenses at Xorfolk.
MERCER, High (1720-1777). an American sol-
dier. He served in the French and Indian war of
1755, and in 1758 was made a lieutenant-colonel. In
1776 he was appointed colonel of the 3rd Virginia
regiment, and the following year was chosen by
Congress brigadier-general. He was mortally
wounded in the night march on Princeton in which
he commanded the advance.
MERCERSBURG, a post-borough of Franklin
county. Pa., ten miles northwest of Greencastle. It
contains Mercersburg College, and was formerly
the seat of Marshall College and a Theological Sem-
inary of the German Reformed church.
^MEREDITH. George, an English novelist and
poet, born in Hampshire, Feb. 12, 1828, and made
his first appearance as an author in 1851 in a little
volume of poems. This was followed by The Sharing
of Shngpat: an Arabian Entertainment, a.h\gh\j origi-
nal tale, in burlesque imitation of the manner of
the Eastern story-teller. The series of Mr. Mere-
dith's greater and more characteristic works began
in 1859 with The Ordeal of Jiichard Eeverel: A Ills-
tor;! of a Father and a Son, a traffic romance, deal-
ing with the larger problems of education, especially
in its ethical aspects. Beauchamp's Career is per-
haps the most perfectly constructed of all the
series. Diana of the Crosm-ays is by general consent
the most charming of Mr. Meredith's novels. Much
of his writing deals more or less directly, in a seri-
ous manner, with the most important problems of
politics, sociology, and ethics. It is in his poetry
1072
M E R I D p] N — MEXICO
that his deepest views of life really find their di-
rectest and most elementary expression.
MERIDEN, a busy inland manufacturing city of
Connecticut, on the Hartford & New Haven Kail-
road, about midway between these cities. The
leading articles of manufacture are britaunia, metal
and silver plated ware, in which it exceeds any
other city of the world. It produces much other
hardware, bronze goods, fire-arms, cutlery, etc.
Population in 1890, 21,230. See Britannica, Vol
XVI, p. 37.
MERIDIAN, a post-village, the county-seat and a
railroad junction of Lauderdale county. Miss.,
eighty-five miles east of Jackson. It has two
female seminaries, machine shop, steam corn-
mills, and manufactories of furniture, doors, sashes
and blinds plows, and cotton yarn. Population,
lo.ssg.
MERIVALE, John Herm.\n, an English scholar
and translator, born at Exeter, 1779, died in 1884.
He was sent to St. John's College, Cambridge, and
was called to the bar in 1805. He contributed
largely so Bland's Collections From the Grerk Anthol-
ogy. From 1831 to the time of his death he held
the office of commissioner of bankruptcy. Works
of no little merit were his Poems, Original and
Translated, and Minor Poems of Schiller. "Charles,
his son, was born in 1808, and educated at Harrow,
Haileybury, and St. John's College, Cambridge,
where he took his decree in 1830. He was chaplain
to the speaker from 1863 to 1869, when he was ap-
pointed dean of Ely. His chief works are the Fall
of the Roman Republic, and History of the Romans Un-
der the Empire. Another son, Hekman, born in 1806,
was educated at Harrow and Trinity College, Ox-
ford, elected Fellow of Balliol, called to the bar in
1832, and appointed professor of political economy
at Oxford, in 1837, and, later, permanent under-sec-
retary of state first for the colonies, next for India.
In 1859 he was made C.B. He died on Feb. 8, 1874.
His son, Herm.in Charles, born in 1839, has writ-
ten a number of successful plays.
MERMAID'S GLOVE {Halichondria Palmata),
the name given to the largest of British sponges.
It grows in deep water, and is sometimes 2 feet
high. It is yellowish and rough, with myriads of
minute fragile spiculse. The surface is very
porous.
MEROM, a post-village ot Sullivan county, Ind.,
on the Wabash River, thirty-five miles lielow Terre
Haute. It is the seat of Union Christian College
(Christian connection).
MERRILL, a city, the county-seat of Lincoln
county. Wis., on Wisconsin River.
MERRIMAC, a village of Massachusetts, on the
Merrimao River, about eight miles northeast of
Haverhill. It is engaged in the manufacture of
shoes and carriages.
MESAGNA, a town in southern Italy, twelve
miles soutliwest of Briiidisi. It produces good
olive-oil. Population, 9,601.
MESENTERY, the broad fold of peritoneum
which attaches the intestines posteriorly to the
vertebral column. It serves to retain the inte.s-
tines in their place, while at the same time it allows
the necessary amount of movement; and it con-
tains between its layers the blood vessels and
nerves which pass to them, the lacteal vessels, and
the nesenteric glands.
MESQUIT. See Mezquitb in these Revisions and
Additions.
MESSENGERS, King's (Queen's), officers em-
ployed by secretaries of state to convey valuable,
and confidential dispatches at home and abroad.
METALLURGY. See Britannica, Vol. XIV, pp.
57-63.
METALS. See Britannica, Vol. XVI., pp. 63-70.
METHODIST EPISCOPAL CHURCH. See
Britannica, Vol. XVI., pp. 185-93. See also Reli-
gious Denominations IN THE United States in these
Revisions and Additions.
• METH UEN, a post-village of Essex county, Mass.,
lying between the New Haven State line and the-
Merrimac River. It manufactures cottons, woolens,
jute, hats and shoes. Population 4,807.
METONYMY (Gr.metonymia, signifying a change
in the name) a figure of speech by which one thing
is put for another to which it bears an important
relation, as a part for the whole, the effect for the
cause, etc. For example, "Lying iips are an abom-
ination to the Lord." This figure is very express-
ive, and is much used in proverbial and other pithy
modes of speech.
METROPOLIS CITY', the county-seat of Mas-
sac county. 111., on the Ohio River, forty miles-
from its mouth. It has a steam-ferry, ship-yards,,
saw and flour-mills.
METTRAY', a village of France, five miles north
of Tours, noted for its great agricultural and in-
dustrial reformatory, the parent of all such institu-
tions. It dates from 1839, and in 1886 had 537 in-
mates.
MEULEBEKE.a town in the Belgian province
of West Flanders, on the Mandel, a tributary of
the Lys, twenty-four miles southwest of Ghent.
Population, 9,063.
MEXICAN WAR. See Britannica, Vol. XVI.,
pp. 219-20; Vol. XXIII, p. 767.
MEXICO, the county-seat of Audrain county,
Mo., 108 miles northwest of St. Louis. It contains
mills and a female seminary. Population, 4,789.
MEXICO, a post-village of Oswego county, N. Y.
It has a tannery, flour and grist mills, foundry and
carriage factories.
MEXICO, Republic of. For general article on
Mexico, see Britannica, Vol. XVI, pp. 206-222.
The latest official estimates of the area and pop-
ulation of IMexico are those of 1889, which furnish
the following figures : Total area of the Repub-
lic, 740,970 square miles; population, 11,632,924, an
increase during the last ten years of 1,724,912.
Constitution and E.xecutive Government. — The
Mexican Constitution now in force, was adopted
Feb. 5, 1857, and modified at diflferent dates down
to 1887. Under its terms Mexico is declared a fed-
erative republic, divided into states — 19 at the out-
set, but at present 27 in number, with two territo-
ries and the federal district^each of which has a
right to manage its own local affairs, while the
whole are bound together in one body politic by
fundamental and constitutional laws. The powers
ot th(> suiireme government are divided into three
branclu's, the legislative, executive, and judicial.
The legislative power is vested in a congress con-
sisting of a house of representatives and a senate,
and the executive in a president. Representatives
elected by the suffrage of all respectable male
adults, at the rate of one member for 40.000 inhabi-
tants, hold their places for two years. The qualifi-
cations re(]uisite are, to be twenty-five years of
age, and a resident in the state. The senate con-
sists of fifty-six members, two for each state, of at
least thirty years of age, who are returned in the
same manner as the deputies. The members ot
both houses receive salaries of 3,000 dollars a year.
The president is elected by electors popularly
chosen in a general election, holds office for four
year.-;, and, according to an amendment of the con-
stitution in 1887, may be elected for two consecu-
tive terms of four years each. Tlie senator who
Iiresides over the senate by monthly election acts
temporarily in default of the president of the Ke-
MEXICO
1073
public. Congress has to meet annually from April
1 to ^lay 30, and from September 17 to December
JO. and a permanent committee of both houses sits
durii)},' the recesses.
President of the Republic, 1891. — General Por-
firio Diaz ; installed president of the Republic, as
successor of General Manuel Gonzales, December
1, 1KS4; reelected and entered his second period of
four years on December 1, 1888. The administra-
tion is carried on, under the direction of the Presi-
dent, by a council of six secretaries of state, heads
•of the departm.ents of justice, finance, the interior,
war and navy, foreign affairs, and public works.
The following table gives the populations of the
Federal (capital city) district and the states
severally, as carefully reported in the general
census of 1879, and as officially estimated by the
State governments in 1889 :
state.
Area in
s.juare
miles.
Population
1879.
Estimated
Population,
1889.
Federal District
Me.\i'-o
4B.?
7,840
1,776
1,622
11.41S
12,019
:i.205
8.161
2.897
23.714
39.174
26.232
2-,5«?
22.999
3,746
16.048
24,552
29,569
11,849
23,637
:«,200
27,916
42,511
25334
83.715
.TO .901
79,020
61.563
11,270
.351 .SM
710,579
1.59.160
138,988
s:«.845
784.466
203.250
427 ,.^50
140,4.30
661.534
983,484
744,000
.542,918
516.486
422..506
65,827
205,362
295,590
302,315
104,747
203,284
18(i,491
140,1.37
190.816
90.413
226,541
130,026
115.424
30,208
4.51,246
778,969
1.51 ,&tO
135,151
l,n07,116
839,468
213,525
494,212
121,926
Tlaxcala
Puebia ...
Querrtaro
Hidalgo
A^uas Calieiites.
Jalisco
Oa.xaoa
1.161,709
806.845
644.157
546,447
526,966
69.547
266.496
3.32.887
282,502
114.028
244.052
223.684
189.1.39
265.931
91,180
298,073
183.327
150.391
34,668
130,019
Vera Cruz
San Luis Potosi
Zacatecas :
Chiapas
Sonera
Ter. Lower Calltornia.
Territory of Tepic
Total
740,970
9,908,011
11.632,924
The chief cities in 1889 reported their popula-
tions thus: Mexico, 329,355; Guadalajara, 95,000;
Puebia, 78,530; San Luis Potos^, 62,573: Guana-
juato, 52,112 ; Leon, 47.939 ; ilonterey, 41,700 ; Aguas
Calientes, 32,355; Merida, 32.000; Oaxaca, 28,827-
Colima, 25,124 ; Vera Cruz, 24,000. In 1887 the num-
ber of Spaniards residing in the country was
9,553. '
Revenue and E.xpexditures. — The revenues and
expenditures since and including 1885, have
been :
Revenue.
18S5-S6 $ 26.770,,S73
1886-87 28,711.817
1887-88 32.321399
1888-,S9 32,745581
1839-90 36,500,000
Expenditure.
188.5-86 $ 31 .672 .8.36
18.86-87 38,78.3,919
1887-88 36.270.448
1888-89 38.527.2:19
36,729.542
The expenditures for 1887-88 and 1888-.89 being
given as approximately correct.
The following are the budget estimates of reve-
nue and expenditure for the year ending June 30,
1891: ^
2—30
Revenue.
Customs $ 26.200.000
Excise 1,500.000
Stamps 9,400.(«i0
Direct taxes 1,400.000
Posts and Tele-
graphs 1,200.000
Mint 270,000
Lotteries 300.00U
Various 1,600,000
Expenditcee.
Legislative power.. $ 1,054,036
Executive '• ... 49,849
Judicial " ... 468,884
Foreign Affairs 471.:i03
Home Department.. 3,678,679
Justice and Educa-
tion 1,424,972
Public works 7,310,320
Finance 11,365,207
War and Kavy 12,629,543
; 41,770,000 % 38,452,803
The Revenue and the expenditure of the varioue
states, according to the latest official data collected
in 1885, balanced at 9,118,977 dollars. In the five
years 1881-85 the total revenues of the States
amounted to 40.163.241 dollars, and of the munici-
palities to 24,323,200 dollars.
The Debt of Mexico.— The debt is held in Eng-
land. On June 23, 1886, arrangements were made
between tlie Mexican government, and the bond-
holders of the several Mexican debts by which the
total amount of the English debt recognized by
Mexico was 22,341,322?., and the arrangement re-
duced it to 13.991,775/. ; ]Mesico, therefore, being re-
lieved by 8,349,597/. On July 1,1889, in accordance
with this arrangement, 411^ per cent of the whole
outstanding debt was redeemed, viz., 40 per cent,
for the capital as per agreement of June 1886, and
\)/i percent, for the interest of the half-year.
On June 11, 1888, the conversion was primarily
closed and another delay given, with the following
results (January 1890) : —
Of the 10.241 .650/. of the 1851 bonds 10,194,000/.
were presented to the conversion. 47,650/. thereby
remaining as deferred. In exchange of the arrears
of interest of the above bonds, new converted bonds
of 1886 were given to the amount of 912.632/. Is. 3rf.
Of the 4,864,000/. of 1864 bonds. 4.792,100/. were pre-
sented to the conversion, and in exchange of them
now converted bonds of the value of 2.595,971/. 158.
were given ; balance not presented is 63.400/.
With other classes of bonds the total of the new
converted bonds issued in London by tlie Mexican
Financial Agency was 4.585.000/.. which, added to
the 1851 bonds— 10,142.400/.— give a total of 14,727,-
400/.
In ^larch 1888 the Mexican government con-
tracted a loan in London and Berlin for 10,500,000?.
in 6 per cent, bonds. Of these. 3.700,000/. were issued
at 78^2. and the proceeds applied by the Mexican
government to the payment of the outstanding
floating debt of the Republic since the year 1882.
The remainder, 6,800,000/.. according to the contract
for the loan, was taken at the option of the con-
tractors befoe July 1,1889, at 86}., per cent. The
contractors gave in exchange one part in converted
bonds, and the proceeds of the other part were ap-
plied to effect the redemption at 41J^ per cent, of
all the outstanding converted bonds in July 1889.
The object (which has been realized) of this part of
the loan was to redeem the 1851 debt and the con-
verted bonds at the rate of 40 per cent., according
to the agreement made between the government
and the bondholders, and referred to above, on
June 23, 1.S86. The conversion of all the internal
debts of the Republic, which is being carried into
effect in Mexico, has reached 31,500,000 dollars and
very little more remained to be converted. The in-
terest on the internal debt for claims not presented
for conversion is, from 1.890, at 3 per cent. All cou-
pons have been punctually paid since 1886. On
ilay 27, 1890, tlie conversion of the old debts was
closed. On September 12, 1890, a new 6 per cent,
loan for 6,000.000/. was issued at 93'.i in London,
Berlin and Amsterdam, the proceeds to be ap-
plied to paying off arrears and balances of rail-
1074
lAI E Y E R — ^l I ALL
way subventions amounting to $40,000,000, assigned
in the form of percentages of customs revenue.
Including this loan the total foreign delit amounts
to 16,500,000/.
The total Mexican debt (including foreign and
home) on Jan. 1, 1891, was $113,600,000.
Akmy axi) Navy. — The army consists of infantry,
22,437; artillery, 2,120; cavalry, 6,359; auxiliary
cavalry, 1,483; rural guards or police, 2,200; gen-
darmery,229; total, 34,833. There are 2,270 olficers.
Every jiiexican capable of carrying arms is liable
for military service from his twentieth to his
fiftieth year.
There is a fleet of two unarmored gun-vessels,
each of 450 tons and 600 horse-power, and armed
with two 20-pounders ; and three small gunboats.
Trade and Commerce — The subjoined table
shows the proportion of precious metal and other
produce of Mexico for several recent years :
The following table shows the principal articles
exported :
Hemp
Coffee
Hides and skius
Woods
Vauilla ^.
Copper
Liviug animals..
Lead
Gum -
Ixtle
Tobacco
Silver
; .872 .593
;,8So,o;j5
;.011.129
1,390,215
92li.903
817,989
587.0fi3
407,787
595,036
594,118
<.1T1.8.SH
1,725,589
Years.
Sundries.
Precious Metal.
Total.
1884-&3
1885-86
18,St;-87
1887-88
18S.8-89
1890-91
13,425,190
13,741,316
15,631,427
17,879.720
21,373,148
23,878,098
$ 33,128,190
29,906,400
83,560,502
31,000,188
38,7&5,27.5
38,621,2.10
$ 46,553,380
43,647,716
49,191,929
48,885,908
60.158,423
62,499,388
The trade of Mexico lies chiefly with the following
the last four years, so far as exports are concerned
ing table includes precious metals :
countries in
; the follow-
Countries.
Exports to
1885-80.
1886-87.
1887-88.
1888-89.
United States....
England
$ 25,429,594
11,600,067
4,936,276
1,571,399
913,2,53
122,192
$ 27,728,714
13,362,187
5,112,521
2,175,760
625,294
187,444
$ 31,059,627
10,540,965
4,474,723
2,177,106
457,842
175,645
$40,853,302
12,535,534
3,496,038
2,061,563
659,330
552.596
Other countries.
MEYER, Conrad Ferdinand, a Swiss poet and
novelist, born Oct. 12, 1825 at Ziirich, near which he
finally settled in 1877. His style is graceful, and
he excells in character-drawing and in genre-pic-
tures of descriptive work.
MEYER, Heinrich August Wilhelm, commen-
tator, born at Gotha, Jan. 10, 1800, died in
Hanover, June 21, 1873. He studied at Jena, was
pastor at Harste, Hoyde, and Neustadt, retired in
1848, and settled in Hanover. His name survives
in his commentaries on the New Testament— a mon-
ument of exegetical science.
MEYER, Joiiann Georg, a German painter, born
at Bremen in 1813. He studied art at Diisseldorf,
and turned his attention to gemr, acquiring great
popularity by his pictures of children. They have
given him the surname of "Kinder-Meyer." Several
of his pictures are owned in the TTnited States.
Among the most noted are: T]ti- Llltic Ilonstirifi:;
The ^'<■ln SIxIcr; What hits Mother Brought^ Little
Briithn- Axlrr),: The Firxt Pmijcr.
MEZZ.WINE, a low story introduced between
two higher ones, or occupying a part of the lieight
of a portion of a high slory. Th(> term is also ap-
plied to the small windows used to light such apart-
ments.
Shipping axd Railway Communications.- — The
shipping of Mexico (now, 1,270 vessels) includes
small vessels engaged in the coast-
ing trade. In the first six months
of 1889, 2,768 vessels of 987,083 tons
(118 of 70,489 tons, British), entered
the ports of Mexico.
In 1890 there were 4.648 miles of
railway open for traffic and 1.369
miles under construction. The capi-
tal invested by English companies
was 14,601,380?., and by American
companies $245,126,249 (U. S.) In
1889 twenty concessions were grant-
ed or amended for railways in va-
rious parts of Mexico. In 1889
there were 12,977,952 passengers,
paying 2,090,505 pesos ; and 875,894
tons of goods were conveyed at a
charge of 4,822,690 pesos.
The total length of telegraph lines
in 1889 was 27.861 English miles, of
which 14,841 miles belonged to the
Federal government, the remainder
belonging, in about equal parts, to
the states, companies, and the rail-
ways. In 1889therewere 1,448 post-
offices.
The inland post carried 87,509,640
letters, newspapers, etc. ; and the
international, ,37,193.403.
MEZZOJUSO, a town of Sicily, in the province of
Palermo, eighteen miles from Palermo city. It is
one of the four colonies of Albanians, who, on the
death of Scanderberg, in the 15th century, iled to
Sicily to avoid the oppression of the Turks. They
preserve their language to a great extent, and fol-
low the Greak ritual, their priests being allowed to
marry. Population, 7,161.
MGLIN, a town of Russia, in the government of
Tchernigov, 125 miles northeast of the town of
Tchernigov. Jlglin has a large cloth-factory, and a
considerable number of German families. Popula-
tion, 5,940.
IMIAGAO, a town on the island of Panay, one of
tlie Philippine Isles, in the province of Iloilo. The
inhabitants, who are industrious, ciuufcirtalile, and
well educated, are estimated at 30,000 in number.
JIIALL, Edward, an apostle of dis-eslablishment,
born in 1809, died at Sevenoaks, Ajiril 29, 1881. He
served as an Independent minister at AVare, and
afterwards at Leicester, down to 1840, when he
founded the "Nonconformist" newspaper. In 1844
he helped to establish the British Anti-State
("hurch .Vssociation, known later as the Liberation
Society, and sat in the House of Commons for
Rochdale, 152-67, and for Bradford, 1869-74. On
M I A M I — M I C H I G A N
retiring he was presented with ten thousand
guineas.
MIAMI, a river of Ohio, which rises by several
branches in the western center of the State, and
after a southwest course of 150 miles through one of
the richest regions of America, and the important
towns of Dayton and Hamilton, empties into the
Oliio Kiver twenty miles west of Cincinnati. It is
sometimes called the Great Miami, to distinguish
it from the Little Miami, a smaller river, which
runs parallel to it, fifteen to twenty miles east,
through the Miami Valley.
MIAMISBUUG, a post-village of Montgomery
county, O., situated in the center of the tobacco
region of iliami Valley. It has fine water-power
several mills and factories, a foundry and excellent
scliools.
MICHEL, Fr.incisque, a learned French anti-
?[uary, born at Lyons, Feb. 18,1809, became in 1839 pro-
essor in the Faculty des Lettres at Bordeaux, and
died May 19, 1887. He earned a great reputation
by his exhaustive researches in Norman history,
French chatisons, the Basques, tiie history of me-
diaeval commerce, and many more among the by-
ways of learning.
MICHELET, Kari, LuDwiG,a celebrated German
author and philosopher, born at Berlin, Dec. 4, 1801,
died in 187IJ. In 1829 he became professor of philos-
opliy in the University of Berlin. His works are of
interest to students of Aristotle and of German
pliilnsonhy.
MICHIGAN CITY, a town of Indiana. Popula-
tion in 1890, 10,704. See Britannica, Vol. XVI., p.
241.
JIICHIGAN LAKE. See Britannica, Vol. XIV,
p. 217; Vol. XXI, pp. 178, 182.
MICHIGAN UNIVERSITY. See Colleges in
these Revisions and Additions.
MICMACS. See North Americ.\n Indians in
these Revisions and Additions.
MICROLESTES, the name given to the earliest
known mammalian form — a marsupial ; it is dis-
covered in the Trias of England and Wiirtemberg.
Only the teeth, wliioh are of small size, have been
met with.
JIICROSCOPE. See Britannica, Vol. XVI, pp.
257-78.
MICROTOME, an instrument for cutting thin
sections of portions of plants and animals prelim-
inary to their microscopic examination. The ob-
jects to be cut are imbedded in some material such
as paraffin or celloidin, or frozen in gum, which
makes the slicing of minute or delicate objects
readily feasible. The instrument is a simple de-
vice by which a sliding razor slices a lixed but ad-
justable object, or by which the object is made to
move up and down across the edge of a razor.
MIDDLEBURY, a post-village, the county-seat
of Addison county, Vt., on Otter Creek. It is the
seat of Middlebury College, has six marble quarries,
good water-power, and manufactures flour, woolen,
cott<m, paper, leather, sash, blinds, and doors.
MIDDLEPORT,a post-village of Meigs county,
Ohio, on the Ohio River.
MIDDLETON, Arthur (1742-1787), a signer of
the Declaration of Independence. In 1775 he be-
camea member of the Provincial Congress, and the
following year was a delegate to the Continental
Congress. In 1880 he was active in the defense of
Charleston, S. C, and after the fall of that city was
for sometime held as a prisoner of war. After his
exchange he served in Congress until the close of
the war. Later he was a State senator.
5IIDDLET0N, a town of Ireland, thirteen miles
east of Cork. At the college (1159G; Curran was
educated. Population, 3,358.
:MIDDLET0WN, a city of Connecticut. Popu-
lation in 1890, 9,012. See Britannica, Vol. XVI, p.
283.
MICHIGAN, State op. For general article on
the State of Michigan, see Britannica, Vol. XVI,
pp. 237-240. The census of 1890 reports the re-
vised area and population of the State as follows :
Area (including 1,485 square miles of water sur-
face), 58,915 square miles; population, 2,093,899,
an increase of 456,952, or 27.92 per cent., during
the last decade. Capital, Lansing, with a popu-
lation in 1890 of 13,102.
The population of the chief cities and towns of
the State having a population of 8,000 or over
were as follows in 1890:
Cities aud Towns.
Adrian
Alpena .'. .
Ann .\rbor
Battle Creek...
Bay City
Detroit
Grand Rapids..
Iron Mountain
Ishpeming
Jackson
Kalamazoo
Lansing
Manistee
Marquette
Menominee .. . .
Muskegon
Port Huron
Saginaw
West Bay City.
Population.
7,849
6,153
8.061
7,063
20,693
116,»40
32,016
(»)
6,039
16.10.5
11,937
8,319
6,930
•4,690
3,288
11,262
8,883
29,441
907
5.130
1,370
6,134
7,146
89,5.36
28,262
5,158
4,693
5,916
4,783
6,882
4,403
7,342
11,440
4.600
16,781
6, .584
11.56
83 37
17.00
86. &5
34.53
76.96
88.27
85.41
29.14
49.es
67.49
223. 30
101.68
62.46
66.81
102.92
* No population in 1880.
The land areas and populations of the several
counties of Michigan, as reported in the census of
1890 were as follows, the areas being in square
miles:
Alcona..
Alger
Allegan .
Alpena..
Antrim..
Arenac..
Barry.
Bay....
Benzie.
Berrien
Branch
Calhoun
Cass
Charlevoix..
Cheyboygan
Chippewa
Clare
Clinton
Crawford
Delta
Eaton. ..
Emmet . .
Genesee .
Gladwin .
Gogebic
Grand Traverse.
Gratiot
Hillsdale
Houghton
Area.
Pop.
1890.
700
5,409
983
1,238
835
38,961
580
15,581
538
10,413
388
5,683
915
3,0.56
580
23.783
466
56,412
340
5,237
570
41,28:)
504
26,791
720
43,501
604
20,953
427
9,686
815
11,986
1,608
12,019
580
7,568
580
26,509
580
2,962
718
15,3.50
580
32,094
438
8,756
640
39,430
510
4,209
1,115
13,166
48.5
13,355
560
28,668
597
,50,660
1,000
35 ,.389
37,815
8,789
6,237
1,8M
26.317
38,081
3,438
36,785
27,941
38,452
22,009
5,115
6,524
5,248
4,187
28,100
1,159
31,225
6,638
39,220
1,127
3076
M I D D L E T 0 W N — M I D D L E T 0 W N
Huron
IngUain
lona
Iosco
Iron
Isabella
Isle Koyal....
JacksoQ
Kalamazoo.
Kalkaska
Kent
Keweenaw —
Lake
Lapeer
Leelanaw
Lonawee
Livingston. ,.
Luce
Mackinac
Macomb
Manistee
Manitou
Marquette . , , .
Mason
Mecosta
Menominee
Midland —
Missaukee -
Monroe
Montcalm.. .
Montmorency
Muskegon —
Newaygo
Oakland
Oceana
Ogemaw
Ontonagon —
Osceola
Oscoda
Otsego
Ottawa
Presque Isle. .
Roscommon . .
Saginaw
Saint Clair. . .
Saint Joseph. .
Sanilac
SchooIVraft. .
Shiawassee . .
Tuscola
Van Buren. . -
Washtenaw. . ,
Wayne
Wexford
Pop. Pop
^••ea. 1890. 18S0.
Indiana Territory,
William Henry Harrison, 1800-6.
Michigan Tebkitory.
28,355
37,666
32,801
15,224
4,432
20,089
33,676
33372
6,873
18,784
135
45,031
39,273
5,160
12,159
55
42,031
34,342
2,937
109,922
2,894
6,505
29,213
7,944
73,253
4,270
3,233
30,1.38
6,253
48,448
20,858
2,455
7,830
31,813
4«,343
22,251
2,902
31,627
24,230
860
39,521
16,385
19,697
12,532
1,334
25,394
10,065
13,973
33,639
10,657
5,048
32,337
32,637
11,987
6,893
1,553
33.624
33,148
40,013
20,476
41,245
15,698
26,586
14,688
41,537
11,699
6,583
3,756
14,630
1,904
4,272
1,914
2.565
10,777
467
1,974
35,358
4,687
2,033
82,273
52,105
33,126
3,113
1,4.'J9
59,095
46,197
25,356
32,589
5,818
30,952
32,508
26,626
26,341
1,575
27,0.59
25,738
30,541
42,210
257414
11,278
30,807
41.848
166,.144
6,815
The list of governors of Michigan, with the dates
of service, is as follows :
Under French Dominion.
Samuel Champlain 1622-.35
M.deMontmagny 1635-47
M.d' Aillebout 1648-50
M. de Lausou 1651-56
M. de Lauson, Jr 1656-57
M. d'AlUebout 16.57-58
M. d' Argenaon 1658-60
Baron de Avaugour 1661-€3
M. de Mesey 1663-65
M de Courcelles 1665-72
M. de Vaudreuil de
Count de Frontenac. . .1672-82
M. de la Barre 1682-85
M. de Nonvllle 1685-89
Count de Frontenac. .1689-98
M. de Cflllieres 1699-1703
M. de Vaudreuil 1703-25
M. de Beauharnois. . .1726-47
M. de Galissonier 1747-49
M.de la Jonquiere 1749-62
M. du Quesne 1752-55
Cavagnac, nXy-«3.
Under British Dominion.
James Murray 176.3-67 I Frederick ITaldlmand. 1777-85
Guy Carleton 1768-77 | Henry Hamilton 1786-86
Lord Dorchester, 1786-96.
Tebritoriai. Governors, Northwest Territory.
Arthur St. Clair, 1796-lSOO.
Governors of the State.
Stevens T. Mason 1&35-40
William Woodbridge .1840-41
J. Wright Gordon 1841-12
John S. Barry 184.3-45
Alpheus Felch 1846-47
William L. Greenly 1847
Epaphroditus Ransom. 1848-49
John S. Barry 1850-51
Robert McClelland. .1852-53
Andrew Parsons 1853-54
Kinsley S. Bingham... .1855-58
Moses Wisner 1859-60
Austin Blair 1861-64
Henry H. Crapo 1865-68
Henry P. Baldwin 1869-72
John J.Bagley 1873-77
Charles M. Croswell. . .1877-81
David H.Jerome 1881-83
Josiah W. Begole 1883-85
Russell A. Alger 1885-87
Cvrus G. Luce 1887-91
Edwin B. Winans 1891-93
Gov. Winan's term of office expires Jan. 1, 1893.
Governor's salary, .$4,000.
Brief Histohic Notes of Michigan. — There are
two opinions as to the origin of the name of the
State. One is that the name is derived from the
Indian words Mitrhi Savyyegan, meaning "lake
country ;" the other is that the word (first given to
the lake) is the Indian equivalent of "fish weir" or
"trap," which was suggested by the shape of the
lake. The present territory had no white inhabit-
ants up to lti41, although French missionaries vis-
ited Detroit about ]()20. The first settlement was
at the Falls of St. Mary in 1641 ; but no permanent
settlement was made until 16R8, when Alouez Dab-
Ion and James Marquette founded the Mission of
St. Mary at St. Mary. A fort was built at Macki-
naw in 1671. A colony was planted at Detroit in
July, 1701, by M. Antoine de la Mottee Cadillac.
France surrendered all its possessions in that
region to England by the treaty of Paris in 1763.
Michigan was included in Canada until it was sur-
rendered to the United States as one of the results
of the Revolutionary war; the formal transfer,
however, was not made until 1796, when Michigan
became a part of the Northwest Territory. When
that territory was divided. May 7. 1800, Michigan
became a part of the Indiana Territory, and Gen.
William Henry Harrison (afterward President of
the United States) became the first governor of the
new territory. Michigan Territory was organized
June 30, 1805. A State constitution was adopted in
1835 and on June 15, 1836, Congress voted to admit
the territory into the Union as a State, on condi-
tion that Michigan should accept the boundary
line claimed by Ohio. Its admission was formally
declared by act of Congress passed Jan. 26, 1837.
The seat of government was transferred from De-
troit to Lansing, INIay 16, 1847.
For numerous other items of recent interest re-
lating to the State, see the article United States
in these Revisions and Additions.
Progress of population in Michigan by decades:
1810, 4,762; 1820, 8,765; 1830, 31,639; 1840, 212,267:
1850, .397,654; I860, 749,113; 1870, 1,184,854; 1880,
1,636,937; 1890,2,093,899.
ailDDLETOWN, a post-village of Newcastle
county, Del. It is a great peach shipping depot and
contains fruit-preserving eslablishments.
MIDDLETOWN, a town of New York. Popula-
tion in 1890, 11,908. See Britannica, Vol. XVI, p.
284.
MIDDLETOWN, a railroad center of Butler coun-
ty, Ohio, thirty-two miles north of Cincinnati. It
contains seven paper-mills, a tobacco factory, flour-
mills, foundry, and a paper bag and scissors factory.
Population 7,637.
^IIDDLETOWN, a post-borough of Dauphin
county. Pa., situated at the junction of Swatarra
creek and the Susquehanna River. It is noted for
MIDDLEWICH — MILFORD
1077
its lumber trade and iron business. It contains the
American Tube and Iron Works, Tusquelianna Iron
AVorks, Middletown Car Works, Cameron Iron Fur-
naces, a furniture factory, and planing mills. Popu-
lation, .5,104.
MIDDLEWICH, an old-fashioned market town of
Cheshire, on the river Dane and the Grand Trunk
Canal, f wenty-one miles east of Chester. Its salt-
manufacture has declined. Population, 3,379.
MIDHAT PASHA{182-'-1884), a Turkish states-
man, born in Bulgaria in 1822. In 1839 he entered
the civil service. In 18o? he suppressed brigand-
age in Roumelia, and was then made a member of
the ministry. In 1860 he was made pasha. After a
short service as governor of Bulgaria he was made
grand vizier. In 1876 he took part in deposing
Abdul Aziz, and again Murad V., who was declared
insane. In 1878 he was made governor-general of
Syria. In 1881 he was tried for complicity in the
murder of Abdul Aziz, and was condemned to
death ; but by diplomatic intervention the sentence
was commuted to banishment to Southern Arabia,
wliere he died in 1884.
MIFFLIN, Thomas (1744-1800), an American
soldier. He was in the Pennsylvania legislature in
1772-73, and in 1774 was a delegate to tlie Conti-
nental Congress. When the news of the fight at
Lexington became known he was made major of
one of the first regiments organized, and shortly
afterward Washington chose him as his first aid-de
camp with the rank of colonel. In 1775 he was
made quartermaster-general, in 1776 brigadier-gen-
eral, and in 1777 major-general. In 1783 he be-
came a member of Congress, and in 1785 was in the
legislature. In 1787 he was a delegate to the con-
vention that framed the United .'States constitution,
and from 1788 to 1790 was a member of the supreme
executive council of Pennsylvania. From 1790 to
1799 he was governor of the State, and then till his
death was a member of the assembly.
MIl'"KLINBURG,a post-borough of Union county,
Pa. It has manufactories of flour and lumber, and
deposits of anthracite and bituminous coal, lime-
stone and iron.
MIGXE, J.\CQUES P.\UL,to whom Roman Catholic
theology owes a great debt of gratitude, was born
at St. FlourinCantal, Oct. 25, 1800, and died in
Paris on his seventy-fifth birthday. He was edu-
cated at the seminary at Orleans, was ordained
priest in 1824, and served some time as curate at
Puiseaux in the diocese of Orleans. A difference
with his bisliop about a lx)ok on the liberty of the
priests drove him to Paris in 1833, where lie started
"L'Univers." In 1836 he sold the paper, and set up
a great publishing house at Petit Montrogue, near
Paris, which gave to the world, besides numerous
•other works of theology, Scriplnrie Sacrse Cursus
Comphtiis and Theologia Cursus (each 28 vols.), Col-
lectiim des Onid-urs Sacres (100 vols.), Pairologia Cur-
>h Compleliis ( Latin series 221 vols., Ist Greek series,
104 vols., 2nd series, 58 vols.), and the Enci/-
clopedle. Thenlogique (171 vols.). Unfortunately,
these editions were prepared too hastily, and do not
possess critical value. The Archbishop of Paris,
thinking that the great undertaking had become a
mere commercial speculation, forbade it to be con-
tinued, and, when the indefatigable director re-
fused to obey, suspended him. A great fire, how-
ever, put an end to the work in February, 1808.
;MIGNET, Francois Auguste Alexis (1796-1884),
a great French historian, born at Aix in Province,
May 8, 1796, studied at Avignon, and then studied
law at Aix with Thiers. In 1821 he went to Paris,
and began to write for the Ceiirrier Franc(iis,!iad to
lecture on modern history at the Athenee. In the
spring of 1824 appeared his Histoire de la JRhohUion.
Franfaise. Mignet joined the staflf of the National,
and with Thiers signed the famous protest of the
journalists on July 25, 1830. After the revolution
of 1830 he became Keeper of the Archives at the
foreign olhce but lost ttiis in 1848. In 1833 he went
on a confidential mission to Spain, and used the op-
portunity to explore the famous Simancas Archives.
Elected to the Academy of Moral ^^ciences at its
foundation in 1832. he succeeded Comie as its per-
petual secretary in 1837, and was elected to fill Ray-
nouard's chair among the Forty in ]t^36. He died
March 24, 1884, within three months of Henri ]\!ar-
tin. Mignet was the first great specialist in Irtnch
history who devoted himself to the complete s-ludy
of particular periods, and in his work he displayed
a marvelous mastery of documents.
MIKLOSICH, Feanz Von, the greatest of Slavonic
scholars, born at Luttenberg, in the Slovenian part
of Styria, Nov. 20, 1813, died in 1891. After study-
ing law at the university of Gratz, hewent in 1838
to Vienna to practice as an advocate, but was led
by Kopitar to the study of philology, and in 1844
obtained a-postin the Impfrial Library. From 1850
to 1885, he was professor of Slavonic at Vienna, in
1851 being elected to the academy of science: and
in 1869 made a "Ritter." His works, nearly thirty
in number, include Eadices Lhigvse Polacoskixenicm;
Lfxicon Linguae Faloposlorenicie; ]'(rglfichende
Orammatik der Slawischen Syrachev (4 vols.), which
have done for Slavonic what Grimm and Diez have
done for the German and the Romance languages;
JJie Bildang der Slavnschen Personettamen; Leber
die Mundarien xmd die Waridennigrn der Ziyevner
Enropas (12 parts) ; Rvmanische Vntersuchungen, and
Etymologlsches ^^'iirterbuch der Slavischen Sprachen.
MILAN, the county-seat cf Sullivan county. Mo.,
250 miles northwest of St. Louis. It has deposits
of fireclay, mineral paint, building-stone, and coal,
and contains a woolen mill, flour-mills, and coop-
erage.
MILAN, a railroad junction of Gibson county,
Tenn., ninety miles northeast of Memphis. It has
cotton and plaining mills, a bigh-Echcol and a
college.
MILEAGE, in the United States, fees paid to offi-
cials, and in particular to members of Congress, for
their traveling expenses, at so much per mile.
There is a fixed table of mileage, and the largest
allowance paid is .$1,440; the total annual cost, for
both houses of Congress, is nearly ^150,000. In
all countries of Europe, except Britain, the same
system prevails with regard to members of the
popular chambers, at least, they being paid either
their traveling expenses or a fixed annual sum.
MILES, Nelson Appleton, an American soldier,
born in 1839. In 1861 he entered the volunteer
service of the United States as lieutenant, and in
1862 became lieutenant-colonel, the same year
colonel, brigadier-general in 1864, and major-gen-
eral in 1865. He became colonel in the regular
Army in 1866, and served in this capacity till the
endofthewar. He then served on frontier duty
until 1880, when he was made brigadier-general and
placed in command of the department of the Col-
umbia. In 1885 he was assigned to the department
of the Missouri, and in 1886 was transferred to Ari-
zona.
MILFORD, a post-village and seaport of Kew
Haven county. Conn., on Long Island Sound. It
manufactures straw goods. Population, 3.800.
MILFORD, a post-borough of Kent county, Del.,
on Mispillion River. It is a shipping point for farm
and orchard produce.
MILFORD, a post-village of Oakland county,
Mich., thirty-five miles northwest of Detroit. It has
a foundry and several manufactories.
1078
M I L F 0 11 h — :\i 1 L K
MILFORD, a post-village of Hillaboroiigh county,
N. H., fifty miles north of Boston, to which city it
ships l!-0,000 gallons of milk annually. It has man-
ufactories of picture and mirror frames, tassels,
furniture, men's boots and shoes, and knitting-
cotton. Here are granite quarries.
MILITARY LAW. See Articles op War in
these Revisions and Additions.
MILITELLO, a town of Sicily, twenty-one miles
southwest of Catania. Population, 10,505.
MILITIA, (from Latin Miles, a soldier), has now
the acquired meaning of the domestic force for the
defense of a nation, as distinguished from the regu-
lar army, wliicli can be employed at home or
abroad in either aggressive or defensive operations.
Every nation has a reserve, under its military law,
upon which its defense would fall on the discomfi-
ture of the regular army ; but the system differs in
each country, and with ttie exception perhaps of
the United States during peace, none are formed
on the model of the British militia. The United
States militia is only national when in the actual
service of the United States Government. Congress
has constitutional power to provide for the organiza-
tion and equipmentof such troopsduring such time,
and the President is then commander-in-chief, and
is empowered to call them out by orders to the offi-
cers appointed by the respective States; while so
employed they receive the pay, rations, etc., of the
regular army. Various acts of Congress require
the enrollment of all non-exempted able-bodied
male citizens between 18 and 45, in every State, and
prescribe the manner of organization, discipline,
etc. The actual or organized militia consisted of,
in 1875:
General officers 119
General Staff officers 88.S
Regimental, Field, and Staff officers l.UCS
Company officers 4,008
Non-commissioned, including musicians and pri-
vates 78.649
Aggregate 84,724
The regularly organized and uniformed active
militia of the several States in the year 1885 aggre-
gated 8-1,739 men ; in the year 188(5 the number was
92,7.^4; in 1887 it had increased to 100,837, and in
1888 it had an available force of 106,814 men.
According to the laws of several of the States,
the State-militia is required to go into camp for
one week in each year. During this time the men
have to conduct themselves like troops of the regu-
lar army. When ever the State authorities request
it, officers of the regular array are detailed to in-
spect these encampments and give instruction to
tiie militia. These officers make afterwards minute
reports of the results of their observations to the
adjutant-general of the United States army. Dur-
ing the year ending Sept. 30, 1888, such encamp-
meut.s were hold in fifteen States, including among
them the tliree largest in the Union.
MILK CELLARS. A cellar dug to the depth of
twelve feet, and having a sub-cellar beneath the
upper one is believed to be the best for milk, in
either summer or winter. There is acertain depth
in the soil where tlie temperature is even llirough
the whole year. This point varies very little from
seven feet from tlie surface, and below this an ex-
cavation from which the air can be excluded will
be tlie best place for a cellar for keeping articles
which are perishable in a warm temperature. Such
a cellar makes safe storage for fruits and vegeta-
bles or for those domestic supplies which re{|uire
such protection. It can easily be kept safe from
dampness by means of a small quantity of quick-
lime in a dish, which will absorb the moiu^ture;
1
and the purity of the air may be preserved by
washing the brick or stone walls with fresh lime
occasionally. Tlie upper part of the cellar will af-
ford every convenience for the dairy-work, as
churning, etc. No part that is below the surface
and in contact with the soil, should be made of
timber.
MILK, Adulteration of. For general article
on Milk, see Britannica, Vol. XVI, pp. 301-306. The
adulteration of milk has re-
cently for obvious reasons, be- j.ji ^j,*
come a question of great im-
portance especially in the
United States. In order to fur-
nish the reader with a practical
as well as scholarly discussion
as to the principal methods used
in this country in testing the
quality of milk, we insert by
permission some interesting
notes from a recent paper by .fs-fTigl-it!' — r.oxt
Henry A. JMott, Jr. E. M., Ph.
D. of New York, published in
the Scientific Ann'rican* Dr. ^; i^j.
Mott first invites attention to I/jd-j]^
the chief appliances for delect-
ing the adulteration of milk.
The Centesimal Galactojie-
TEK was inventedby iJinocourt :
it is shown in the figure. The
stem of the instrument has two
scales: one for pure milk, the
other for skimmed milk ; the
scale A, in part colored yelloir^
serves to weigh the milk with
its cream ; the first degree on
the top of the scale is marked
50, which corresponds to the sp.
gr. 1-014. The following marks
extend from 50 to 100 (sp. gr.
l'OL'9), and over. Each degree ■
starting from one hundred in
mounting up to 50, represents a
hundredth of pure milk; the degrees formed by a
line are equal, as 50, 52, 54, etc. ; the degrees formed
by a dot are unequal, as 81,83, 85, etc. To illus-
trate by an example: If the galactometer is sunk
to the 85th degree, that will indicate 85hundredtlis
of pure milk, and consequently that 15 hundredths
of water has been added to this milk ; if sunk to 60
degrees, that will indicate 40 hundredths of water,
or four-tenths of water added. If it is desired to
count by tenths, it is only necessary to notice that
the first tenth is white, that the second is colored
yellow, the third white, the fourth yellow, and
that the fifth is also white; toward the middle of
each tenth the figures 1, 2 3, 4, 5 are placed to in-
dicate their order.
The scale, o, is in part colored blue, and is des-
tined to weigh skim milk; it is, like the first, di-
vided into hundredths (100 degrees), of which the
first 50 have been cut off as useless, as in the case
of the other scale, each degree commenoing from
100 to 50 and mounting upwards represents a hun-
dredth of pure skimmed milk, consequently the
mannerof estimating the quantity of water added
to skim milk is absolutely the same as for pure
milk with cream. The degree 130 corresponds to a
specific gravity 1'038, the degree 120 to T035, the
degree 110 to r032, the rf,v/)v<- 100, >ehieh t.-^ the
Htiiuddi-d, to 1-029, the degree 80 to 1-023, the degree
70 to 1020, the degree 60 to 101 7 and the degree 50
to 1014.
* For an extended discnsK'on of the suhjoot the profession-
al inquirer is referred to Suiuntiflc American in loc.
M I L K
1079
a
iP
Another Centesimal Galactometer was invented
by Chevallier; it is similar to the above instrument.
It serves to determine the specific gravity of cream,
millt, and skimmed milk. This instrument is used
in connection with the creamometer. The specific
gravity of the milk not skimmed is first deter-
mined, noting the temperature, then the volume
of cream is ascertained by means of the cream-
ometer, and finally the specific gravity of the
skimmed milk is determined, noting the tempera-
ture.
from the data obtained, by referring to tables
compiled by Chevallier, the additional water con-
te itiiof the milk is ascertained.
The fjAt'ToDEsiMETBR. — This is an instrument dif-
eriri .' from the galactometer just described only in
the division of its scale. It is the pro-
duction of Bouchardat andQuevenne, and
is represented in the figure. This instru-
ment, like all the densimeters, gives im-
mediately and without calculation the
density of the liquid in which it is plung-
ed; its scale comprises only the densities
which may be presented by pure or adul-
terated milk. The shaft bears three dis-
tinct graduations. The first, which is the
fp middle one in the figures, contains the
whole numbers intermediate between 14
and 42. In reality, the whole numbers
comprised between 1014 and 1042 ought
^ ^^ to be inscribed; but on account of the
»lNti small size of the shaft the two first figures
have been suppressed which do not change.
If, consequently, the instrument is sunk
in a liquid up to the figure 29, this signi-
fies that a litre of thismilk weighs 1029
grams, and that its density is conse-
nuently 1029. The instrument has been
graduated for the temperature of -r 15°
C. It is necessary, therefore, for obtain-
ing an f.rnct indication, to be assured the
liquid under examination is at this tem-
perature. In the contrary case, it may
be brought back to this degree by plung-
ing tlie gauge containing the milk in
water tliat is cold, or in lukewarm water,
according as the thermometer is above or
below -f 15°. The scale on the right i.s
employed when it is certain that tlie milk acted on
is not skimmed. This scale shows what are the
variations of tlie density of milk in proportion as
water is added, and the figures yo, x^s, etc., indicates
that the liquid operated upon has been mixed with
this proportion of water. The scale on the left
contains the same indications relative to skimmed
milk. Milk is marked pure on this instrument, be-
tween the specific gravities 1030 and 1034, skimmed
milk is marked pure between the gravities 1034
and 1037.
The Lactometer. The original lactometer was
discovered by Prof. Edmund Davys in 1S21. It is
represented in the figure. It is made of brass, and
consists of a pear-shaped bulb, at the top of which
is a graduated stem, and at the bottom a brass
wire, to the end of which a weight is screwed. This
instrument is only intended for skimmed milk, and
the 0 mark corresponds to the sp. gr. 10.35, which,
according to Davy's experiments, represents the
lightest genuine skimmed milk. The dots in the
figures, which extend from 0 to 35, indicate parts
of water in 100 parts skimmed milk at 60°.
Who invented the lactometer for testing milk I am
unable to ascertain ; one thing is certain, however,
the one who first divided the scale from 0 water to
100 pure milk was, of course, the inventor. Of the
various lactometers that have been in use, the only
difiference was the specific gravity represented by
the 100 degree of the scale. The specific gravity
corresponding to the 100 degree on the centesimal
galactometer invented by Dinocourt, as I have
already stated, was 1029, which was intended to
represent the proper minimum. This sp. gr. has
been adopted by the Board of Health of New York
as the standard for their lactometers.
The old standard adopted by tlie milk dealer was
1.030; this was changed by Dr. Chilton to 10.34, and
has gradually dropped to 1033. So that the stand-
ard now employed by the milk dealers to secure for
thernseh-es pure milk is 0004 higher than that
adopted by the Board of Health.
In graduating the board of health lactometer
shown in the figure, the 100° is placed at the stand-
ard 1 029, and 0 at 1 000, the gravity of water, the
intermediate spaces being divided into 100 equal
divisions. Great care should be taken to deter-
mine with absolute accuracy
the 0 degree and the 100 de-
gree; other points may also
be determined, but they are
not alisolutely necessary if
the space is properly divided.
- e—^ju
The point to which the lactometer sinks ia
the milk under examination indicates the per-
centage of milk in 100 parts. Thus, if the
lactometer sinks to 80, the milk must consist
of, at least, 20 per cent, of water and 80 of milk.
This assumes the original milk to have had a speci-
fic gravity of 1029; but, if the milk had originally
a gravity of 1 034, it would require 1667 per cent,
of water to bring it down to 1 "029, and 20 per cent,
more water to lower it to 80° on the lactometer.
The temperature at which examinations are made
with the lactometer should be 60 F., for exact de-
terminations, as the instrument is graduated for
that temperature. If it is only necessary to estab-
lish the fact of an adulteration by water, the milk
may be cooled to a temperature below 60° F., which.
1080
MILKWORT S
an expert can easily ascertain by the sense of taste,
etc. — tlie lower the milk is cooled the more dense
it becomes ; consequently, if tlie lactometer should
sink below 100 in a sample of milk known to be be-
low 60° F., suilicient evidence to establish the fart
of its adulteration is indicated. A sample of milk
tested by Dr. Chandler, of New Vork, which stood
at 100 by the lactometer at 60° F., was found to
stand at 106 at 44° F., at 98 at 66° F., at 90 at 80°
P., and at 74 at 100° F.
V.\LrE OP THE Degrees of the Board of Health
Lactometer in Specific Gravity. — By
Dr. Waller.
c
C
c
%
"S
^
i
Gravity.
a
Gravity.
a
Gravity
a
Gravity.
^3
§
1
§
%
'-'
J
1 '-'
►J
0
1-00000
31
1-00899
61
1-01769
91
1-02639
1
1-00O29
.32
1-00928
62
1-01798
92
1-02668
2
1-00058
33
1-00957
63
1-018-27
93
1-02697
3
1-00087
34
1-00986
64
1-01856
94
1-02726
4
1-00116
35
1-01015
65
1- 01885
95
1-02755
5
1-00145
36
1-01044
66
1-01914
96
102784
6
1-00174
37
1-01073
67
1-01943
97
1-02813
7
1-00203
38
1-01102
68
1-01972
98
1-02842
S
100232
39
1-01131
69
1-02001
99
1-02871
9
1-00261
40
101160
70
1-02030
100
1-02900
10
1-00290
41
1-01189
71
1-02059
101
1-02929
11
1-20319
42
1-01218
72
1-02088
102
1-02958
12
1-00348
43
1-01-247
73
1-U2U7
103
1-02987
13
1-00377
44
1-01-276
74
1-02146
104
1-03016
14
1-00406
45
1-01305
75
1-02175
105
1-0.3045
15
1-00435
46
1-013.34
76
1-02204
106
1-03074
16
1-00464
47
1-01303
77
1-02233
107
1-03103
17
1-00493
48
1-01392
78
1-02262
108
1-03132
18
1-00522
49
1-01421
79
1-0-2291
109
1-03161
19
1-00551
50
1-01450
80
1-02:520
110
103190
20
1-00580
51
1-01479
81
1-02M9
HI
1-03219
21
1-OOS09
52
1-01508
82
1-02378
112
1-03248
22
1-00638
,53
1-01537
S3
1.02107
113
1-03-277
23
1-00667
54
1-01.566
M
1-02436
114
1-03306
24
1-00696
55
1-01595
85
1-0-2465
115
1-03335
25
1-00725
56
1-016-24
86
1-02494
116
1-03364
26
1-00754
57
1-01653
87
1-02523
117
1-03393
27
1-007*3
58
1-01682
88
1-0-2.552
118
1-03122
28
1-00812
59
1-01711
89
1-02581
119
1-03151
29
1-00841
60
1-01740
90
1-02610
120
1-03480
30
1-00870
The following table by De Voelcker (with an ad-
dition by Dr. Chandler, of the 2d column), illus-
trates the effects of watering and skimming:
UNSKIMMED. SKIMMED.
Sp. Gr. Lact. Sp. Gr. Lact.
Pure milk 1-0314 108 1-0337 117
10 per ceut. water added.. 1-0295 102 1-0308 106
20 " " " . . 1-0257 88 1-0265 91
30 " •' " .. 10233 80 1-0248 86
40 " " " .. 1-0190 66 10208 72
50 " " " .. 1-0163 56 10176 60
Thus it is seen that with a sample of pure milk of
sp. gr. 1-0.314 more than 10 per cent, of water
could be added before the gravity is reduced to
rOL'9 or 100 on the lactometer; and after skimming,
considerable more.
That tlie specific gravity 1-029, is the true minimum
standard for yure whole cdiu's milk, I think I have
already fully demonstrated, yet it is interesting to
bear in mind that it has been confirmed by
"Miiller, Fleischmann, Goppelsroeder, Kramer, and
other specialists."
Miiller says : "From more than 6,000 notes by
Quevenne and Bouchardat, the minimum is 1029,
and the maximum 1-033. For the hospitals and
puljlio institutions in Paris, the minimum is 10.30-"
He further says: "If," . . . "we go through all
Europe, from country to country, from place to
place, from dairy to dairy, from Alp toAiii, with
the lactodensimeter in hand, and mix at times the
milk of several cows together which have been
milked under conditions sufficiently touched upon,
we shall find that tlie milk which is divided as a
trade commodity from the physiological milk
weighs between f029 and fOSS."
Let us consider, noiv, if there are any objections
to the use of the standard lactometers for the de-
tection of adulteration. I have already stated that
a samjile of perfectly pure cow's milk, possessing a
high specific gravity, can be considerably addi-
tioned with water, and the lactometer is unable to
detect the fraud. The question naturally arises, is
there any method by \vhich the fraud can be de-
tected? The ans-wer comes, unfortunately, vo —
owing to the variation in the proportion of each
constituent, a proper margin has to be left for the
maximum and minimum proportions, and between
these limits the fraud can be perpetrated, and
defy all science to detect it.
Milk may be skimmed, -which will increase'the
specific gravity of the fluid ; it may then be water-
ed, and the sp. gr. reduced to the standard of the
lactometer, or the sp. gr. may be still further re-
duced, and by the addition of some solid substances,
such as sugar or salts, increased to the standard
specific gravity. The question naturally arises
here, can the lactometer detect such adulteration?
To answer this question -ue must first inquire into
the method adopted, where the lactometer is used
to detect adulteration. It is to be supposed (hat
an expert commissioned to examine milk for adul-
teration, using as a means, the lactometer, will
perform the testwhicli is to be made, in connection
with the senses, that is to say, the sample under
examination should be examined as to its opaque-
ness and color, its taste and odor, etc. If on the
contrary, he performs the task automatically,
simply taking the degree of the instrument, noting
the temperature, without examining the sample
otherwise, the lactometer itself will not detect such
adulteration; but such an experimenter is not fit
or competent to make such investigations, for, no
matter -what the method of examination may be,
the common sense is always required to accomplish
the obi'ect in view. I say v lih(nit fear of si ccessfvl
vohiraeliction, that if the lactometer is used in
connection with the senses, that is to say, regard-
ing the flow of milk from the bulb ofthe instru-
ment, observing its opacity and color, as also ex-
amining as to flavor and odor of the sample under
examination, the lactometer will detect all the
practical frauds perpetrated hii milknwii. In my
opinion there is not one unprejudiced person, with
the experience and education tliat the milk expert
should have, that cannot distinguish a fair sample
of pure milk from a fair sample of skimmed milk
or cream ; and if such is tlie case, how readily
could be detected an adulterated sample.
In the first part of this paper I stated that the
indications of the lactometer are infallible; this is
the case, for if a sample of milk should indicate a
degree less than the standard, there is indisputable
evidence that the sample has been t:impered w-ith.
:\nLKAVOKTS (so called from the milky juice),
various species of plants belonging to the natural
order I'dli/rjalcr or Pohj<jolacra: The order com-
prises about twenty genera and 500 species which
are widely distributed over the trojiical and sub-
tropical world ; several species are natives of North
America and Europe. They are herbaceous plants
or shrubby. The leaves are usually simple and
destitute of stipules; the flowers irregular. They
are generally tonic and slightly acrid, and some
are very astringent. The common Milkwort
.M 1 T. L — M I L I T A R Y ACADEMIES
1081
(Polygala vulgaris) is a small perennial plant, with
an ascending stem, linear-lanceolate leaves, and a
terminal raceme of small beautiful dowers. It
varies in sine and in the flowers and leaves. P.
Senega is a North American species, with erect
simple tufted stems about one foot high, and ter-
minal racemes of white flowers. The root is the
Snake Root of the United States, famous as an
imaginary cure for snake-bites, but really possess-
ing important medicinal virtues. See Britannica,
Vol. XXI, p. 189. The root of P. poaya, a Brazilian
species with leathery leaves, is an active emetic.
P. tincloria, a native of Arabia, furnishes a blue
dye like indigo. Another medicinal plant of the
order is the Kattany Root.
MILL. See Britannica, Vol. IX., pp. 343-47.
MILL (Lat. niille, a thousand), in the United
States, the tenth part of a cent the thousandth part
of a dollar. As a coin it has no existence.
MILLAIS, Sir John Everett, a celebrated Eng-
lish painter, born at Southampton, .Tune 8,1829, the
descendant of an ancient .Jersey family. In the
winter of 1838-39 Millais began to attend the draw-
ing academy of Henry Sass, passing, two years
later, into the schools of the Royal Academy. At
the age of seventeen he exhibited at the Royal
Academy his "Pizarro seizing the Inca of Peru,"
ranked by competent critics of the day as on a
level with the best historical subjects then shown.
His first pre-Raphselite picture, a scene from the
Isabella of Keats, strongly recalling the manner of
the early Flemish and Italian masters, figured in
the Academy in 1849. In 1856 he was elected an
Associate of the Royal Academy, and soon after-
wards he exhibited three of the richest and most
poetic of the productions of his pre-llaphaelite
period, namely, the Anttimn Leaves in 1856, the
Sir Isumbras at the Ford in 1857, and The Vale of
Rest in 1859. In the finer of the works which fol-
lowed, the precision and clear definition of pre-
Rapha;lite methods still survive ; but in the ex-
quisite Gambler's ir/Jc tiiere became visible a larger
and freer method of handling, wliich is yet more
fully established in The Boyhood of Raleigh, a pic-
ture which marks the transition of his art into
its final and most masterly phase, displaying all
the brilliant and efifective coloring, the effortless
power of brush-work, and the delicacy of flesh-
painting, in which he is without a modern rival.
Millais has executed a few etchings, and his innu-
merable illustrations, dating from about 1857 to
1864, place him in the very fir.st rank of woodcut de-
signers. He is a D. C. L. of Oxford ; in 1885 he was
created a baronet.
MILBURX, Wn.Li.\.M Henry, an American cler-
gyman, born in Philadelphia, Sept. 26, 1823. When
a boy, although of defective sight, he studied at Illi-
nois College ; at the' age of 20 became a Methodist
preacher ; was chaplain to Congress ; in 1859 went to
England and lectured with success ; on his return
was ordained in the P. E. Church, but in 1872 re-
turned to Methodism. He is widely known as the
"blind preacher," and has published some able
works.
MILITARY ACADEMIES. The Military Acad-
emy of the United States is at West Point, N. Y., on
the Hudson River. It was founded by act of Con-
gress, March 16,1802. At first it consisted of fifty
cadets, forty of them being attached to the artil-
lery and ten to the engineer service. This was the
nurleus to which various additions were made until
1812, when the institution became substantially
what it is at present. Tlie staff of instruction and
government consists of, 1. The superintendent of
instruction and military staff; 2. The comman-
dant of cadets and six assistants; 3. eight non-com-
missioned officers, and one professor with thirty-
two assistants. Each Congressional district and
territory is entitled to one cadetship, and the Pres-
ident appoints ten cadets annually, who must be
between the ages of 17 and 22. Tliose admitted
bind themselves, by special articles, to serve the
United States for eight years unless sooner dis-
charged. The course of study, which is very
thorough, especially in the mathematical depart-
ment occupies four years, and the discipline, in-
tended to secure habits of prompt, implicit obedi-
ence to lawful authority, as well as habits of neat-
ness, order and regularity, is more strict even than
that of the army, or that in any similar institution.
At graduation the class is divided into three grades,
according to scholarship, and recommended for
promotion, according to this schedule, in different
corps, and commissions for the rank of second lieu-
tenant conferred.
In order to superadd a special professional train-
ing for the graduates of the military academy, and
also to give the needed opportunity to those who
have received their commissions from civil life or
from the ranks of the army, post-graduate schools
WEST POINT PARADE GROUNDS.
have been opened at Fortress Monroe, Fort Leav-
enworth, and at Willet's Point. These schools are
also maintained by the United States government.
The School at Fortress Monroe, la., was commenced
in 1867. It has a two-years' course. It is intended
for subalterns of artillery, yet officers of other
arms of the service have, by special permission of
the secretary of war, been educated there. The
School at Fort Leaeenworth, Kan., began in 18S2. It
is designed for the training of infantry and cavalry
officers. The School at Willet's Point, iV. }'., was es-
tablished in 1865. It is intended for the education
of officers of the engineer corps and also of artillery
officery. The course is for two years. Special at-
tention is given to permanent works, their con-
struction and management; also to torpedoes and
the electrical service.
Other Milit-^ry Colleges and Schools. — The
most notable military school maintained by a State
is the Virginia Military Institute. It ranks next to
the United States Academy. This school is located
at Lexington, Va. It has eight professors, and is
modelled after the West Point school in its general
plan, instruction and discipline. It has usually
about 1.50 students.
The Kentucky Military Institute is simil&T. It has
its existence since 1846, first at Frankfort, and now"
1082
I\I I L L B R 0 0 K — .M I L N E - E D W A R D S
at Farmdale, Ky. It has eleven professors and in-
structs usually about 130 students. There are a
number of other military schools, especially in the
southern States ; some are also maintained pri-
vately in New York, INIassachusetts, Vermont, Penn-
sylvania, Ohio, and Michigan.
Since 1883 the general government details forty
non-commissioned officers of the army to act as pro-
fessors of military science and tactics at certain
designated colleges which had accepted from the
United States certain grants of land for education-
al purposes. It had been stipulated in the grants,
and made obligatory upon each college so helped,
to embrace military training in its course of in-
struction. These officers are distributed among
the several States as nearly as possible according
to the population. Recently, however. State insti-
tutions which introduce a military branch of in-
struction are preferred in the distribution of these
military instructors.
During the year ending Sept. 30, 1888, forty insti-
tutions in different parts of the Union availed
themselves of the opportunity of giving instruction
in military science, with practice in military drill,
to such of their pupils as chose to receive it. The
whole number of students over 15 years of age at-
tending these institutions was 7,791. Of this num-
ber about 4,000, or 51 per cent., attended infantry
drill. During the previous year the same system
had been pursued. The total number of students
was, however, less, and only 49 per cent, had at-
tended the drills. This shows that the interest of
the students in military matters is increasing.
MILLBROOK, a manufacturing town of Durham
county, Ontario, eighteen miles from Port Hope.
MILLBURY, a post-village and railroad junction
of AVorcester county, Mass., on Blackstone River,
six miles south of Worcester. It manufactures
cotton and woolen goods, stockings, cutlery, cast-
ings, shoes, W'hips, lumber, and carriages. Popula-
tion, 4,427.
MILLEDGK, John (1757-1818), a United States
statesman. He took part in the Revolutionary
war on the side of the colonies, and was appointed
attorney-general of Georgia in 1780. From 1792 to
1802 he was a member of Congress, except in the
years 1799 and 1800, and then till 1806 was gov-
ernor of his State. From 1806 to 1809 he was a
United States Senator.
MILLEDGEVILLE, the former capital of Geor-
gia, a city and the county-seat of Baldwin county.
It is in a cotton-growing region, has cotton manu-
factories, the State lunatic asylum. State peniten-
tiary, and the Middle Georgia Military and Agri-
cultural College. Population, 3,306.
MILLER, CiNCiNNATus HiNER (Jo.\quin), an
American poet, born in 1841. He began the prac-
tice of law in 1863, and from 1866 to 1870 was judge
of Grant county, Oregon. He then devoted him-
self entirely to literature, and has written several
plays, including The Danites. Among his poems are
Noiig.s of the Sierras (1871); Songs of the Sunlands
(1873); Songs of the Desert (1875); and Songs of the
Mexican Seas (1887). His prose works are The Baro-
ness of New Fori (1877); IVie Danites in the Sierras
(1881) ; Shadotos of Shasta (1881); Memorie and Rime
(1884); and '49, or the Gold Seekers of the Sierras
(1884).
MILLER, .Joseph, an English comedian, born
al)Out 1684, died in 1738. In 1739 a collection of stale
jokes was made by John .Alottley and published as
Jue Miller's Jests, and it is by this work that he is
best known.
MIlJyER, Samuel, a distinguished American di-
vine, born near Dover. Del., in 1769, died at Prince-
ton, N. J., in 1850. He was professov of ecclesiastical
history at Princeton, from 1813 to 1849. He wrote
numerous polemical treatises, and some valuable
historical and biographical works.
MILLER, Wakner, an American statesman, was
born in Oswego county, N. Y., Aug. 12, 1838. He
served with credit in the civil war; was elected to
the New York assembly in 1874, to Congress in 1878,
and became United States Senator in 1881. He was
the Republican nominee for governor of New York
in 1888. He is president of the Nicaragua Canal
Company.
MILLER, William Allex, an English chemist,
born at Ipswich in 1817, died in 1S70. He is best
known by his valuable Elements of CJiemistvu.
INIILLER, William Hallowes (e 1801-1880), an
English mineralogist and physicist. In 1843 he
superintended, by order of parliament, the con-
struction of standards of weight and length, the
old standards having been destroyed by fire. In
1870 he served on the international commission upon
the metric system. He was a prominent member
of tlie principal scientific societies of the world.
MILLERSBURG, the county-seat of Holmes
county, Ohio. It contains a flour-mill, a foundry,
and a machine shop.
MILLERSVILLE, a post-village of Lancaster
county, Pa. It contains the Millersville State Nor-
mal School.
MILLIARD, the French collective name for a
thousand millions; familliar in connection with the
five milliards of francs (5,000 millions of francs, or
$1,000,000,000) paid by France as war indemnity to
Germany in 1871-73.
MILLIKEN'S BEND, a village of Louisiana,
about 15 miles above Vicksburg, the scene of an en-
gagement in June, 1863, between the Confederates
under General McCullough, and a body of colored
troops, in which the former, owing to the timely
arrival of Porter's fleet, were repulsed.
JIILLS, Clark (1815-1883), an American sculptor.
For several years prior to 1835 he was in the stucco
business in Charleston, S. C, and then resolved to
try cutting in marble. His first work was a bust
of John C. Calhoun, for which he received a gold
medal from the city council, and it was placed in
the city hall. Subsequently he executed busts of
several eminent men of South Carolina, and in 1848
made the model for the equestrian statue of An-
drew Jackson, which stands in Lafayette Square,
Washington, D. C. Air. Mills has since executed
several other popular statues, besides many busts.
MILLS, Samiel John (1783-1818). an American
clergyman. In 1812-13 he was exploring agent of
the Massachusetts and Connecticut Missionary So-
cieties, and in 1814-15 missionary and Bible agent.
In 1817 he was chosen to explore the coast of west-
ern Africa in behalf of the American Colonization
Society. He reached Africa in the early part of
1818 and after two months on that continent began
his homeward voyage. He died while at sea.
MILLTdWN, a post-town in Charlotte county, N.
B., on St. Croix River. It is a great lumber depot.
MILMOIIE, Martin (1844-1SS3), an American
sculptor. He entered the studio of Thomas Hall in
1860, and several years later opened a studio of his
own in Boston. Among his works are soldiers' and
sailors' monuments in several cities, busts of I'ope
Pius IX., Charles Sumner, Wendell Phillips, Ralph
Waldo Emerson, Longfellow, Theodore Parker and
Oieorge Tickner, besides the ideal figures Ceres,
Flora, I'uniona, Ameriea and Weeping Lion.
AIILNE-EDWARDS. Henri, a French naturalist,
born at Bruges, Oct. 23. 1800. died July 29. 1885.
His father was an Kngli.<hmaii. Milne-Edwards
studied medicine at Paris, where he took his degree
of Jl. D. in 1823, but devoted himself to natural his-
M I L N E R — M I N I E
1083
tory. He was elected in 183S member of the Acad-
■dmie des Sciences in the place of Cuvier. In 1841
he iilled the chair of Entomology at the Jardin des
Plantes, and in 1844 became professor of zoology
and physiology. He published numerous original
memoirs of importance in the Annales dea ScUnicc^
Naliircllfs, a journal he himself assisted in editing
for 50 years.
His Elements de Zoologie had an enormous circu-
lation, and long formed the basis of most minor
manuals of zoology published in Europe. His Lcc-
tures on the Physiology and Comparative Anatomy of
Man and the Animals (14 vols.) have a great perma-
nent value for their immense mass of details, and
copious references to scattered sources of informa-
tion. His researches in the distribution of the
lower invertebrates led him to the theory of cen-
ters of creation ; and to this he adhered through-
out life, in spite of the general acceptance of the
newer and larger views of Darwin by his fellow-
scientists. His elder brother, Frederick William,
was almost equally celebrated. He founded the
Ethnological Society in Paris, and is considered the
father of ethnology in France.
MILNER, Is.\AC, an English author and scholar,
born near Leeds in 1751, died in 1830. He was a
brother of Joseph Jlilner, whose Church History he
brought down to a later date.
MUvNER. Joseph, an ecclesiastical historian,
born near Leeds in 1744, died Nov. 15, 1797. He
studied at Catharine Hall, Cambridge, and after-
■hards became well known as head-master of Hull
grammar-school. He was vicar of Forth Ferriby
seven miles from Hull, and lecturer in the princi-
pal church of the town, and in 1797 became vicar
of Holy Trinity Church. Milner's principal work
is liis History of the Church of Christ, of which he
lived to complete three volumes, reaching to the
13th century ; a fourth volume coming down to the
16th century, was edited from his MSS.
MILREIS, or MiLR.tES, a Portuguese silver coin
and money of account, contains 1,000 reis. The coin
is commonly known in Portugal as the coroa, or
"crown," and is the unit of the money system in
that country. It is also used in Brazil.
Milton, a city, the county-seat of Santa Rosa
county, Fla., on IJlackwater River. It contains
foundries, and a dry dock, and has a large lum-
ber trade.
MILTON, a post-village of Norfolk county, Mass.,
nine miles south of Boston. Ice and building-
stones are l)ere obtained, and paper, leather, choco-
late, and rul)ber-goods are manufactured. Market
gardening is largely carried on in the vicinity.
Population, 4,278.
MILTON, a post-borough of Northumberland
county. Pa. It has manufactories of lumber, and
contains car-works, machine shops, agricultural
works, and foundries; also a rolling-mill and a nail
factory. Population, 5,317.
Milwaukee, a city of Wisconsin, the com-
mercial metropolis, railroad center, and port of
entry of the State, ^'ilwaukee is one of the
greatest wheat markets in the country ; it has ex-
tensive manufactories of iron, flour, malt liquors,
and leather. From its elevated position it over-
looks Lake Michigan. It is noted for the health-
fulness of its situation. Population in 1890, 203,979.
See Britannica, Vol. XVI, p. 340.
MINAS, the capital of a wild, mountainous pro-
vince (area, 4,844 square miles ; population, 23,000),
of the same name in southern Uruguay, seventy-
five miles by rail northeast of Montevideo. Pop-
ulation, 7,000.
MINDEN. a post-village, the capital of Webster
parish, in the northwestern part of Louisiana.
Cotton and lumber are the chief articles of ex-
port.
MINDERERUS SPIRIT, a valuable diaphoretic,
much used in febrile diseases. It is prepared by
adding ammonia or the carbonate of ammonia to
acetic acid till a neutral liquid is obtained. It is
sometimes applied hot on flannel in cases of mumps,
while it has also been employed as an eyewash in
chronic ophthalmia.
I\1INE0LA, a flourishing town of Texas, and an
important railroad junction, situated about a hun-
dred and twelve miles west of Shreveport, Louis-
iana, at the intersection of the Texas and Pacific
and the Missouri Pacific railroads.
MINER, Al.\nzo A., an American clergyman and
temperance advocate, born in New Hampshire in
1814. He has lield many important offices con-
nected with education ; and has been a voluminous
writer, especially in the anti-slavery and temper-
{ince causes. He was president of Tufts College
from 1SR2 to 1875.
MINERAL POINT, a city of Iowa county, AVis. It
contains grist-mills, foundries, a car-shop, and
zii.c and lead furnacef. Population, 2,C94.
:MINERA1> WOOL, when a jet of steam is al-
lowed to escape through a stream of liquid slag.the
slag is blown into very fine white threads, called
"mineral wool," which is used as a covering for
steam-pipes and steam-boilers ; as a deafening for
floors and buildings; and, generally, as a non-con-
ductor of heat.
:MINERSVILLE, a post-borough and a railroad
junction of Schuylkill county, Pa., on the west
branch of the Schuylkill River. Coal-mining is
the chief industry, and the town contains water-
works, a fire department, foundries and an an-
thracite furnace. Population, 3,502.
MINGPIETTI, Marco, an Italian statesman, Ca-
vour's disciple and successor as leader of the
Italian Right, born Sept. S, 1818, died at Rome
Dec. 10, 1886. He supplemented a brilliant course
at his university by a prolonged tour in France,
Germany and Great Britain. With the election
in 1846 of Pope Pius IX. I\Iinghetti started a jour-
nal in aid of his country's regeneration. In 1859-60
he was Cavour's secretary for foreign affairs. His
next post was that of minister of the interior, and
on Cavour's death in 1801 he was regarded as his
ablest representative in the Italian chamber. In
1863 he became prime-minister, in 1864 -he con-
cluded with the Emperor Napoleon the "Seiitem-
ber Convention." In 1868 he was Italian minister
in London, and thereafter minister of agricul-
ture. In 1870 the collapse of the Second Empire
brought with it the dissolution of the September
Convention, and Rome became the capital of Italy
and seat of government. From 1S73 to 1876 Min-
ghetti was prime minister for the second time, and
among many useful measures earned his country's
gratitude by effecting the "paraggio" or financial
equilibrium between her outlay and income. For
the next ten years Minghetti was still the most
prominent member of the Italian parliament.
His lectures and essays on Raphael and Dante
illustrate on the {esthetic side a catholicity of
culture which in the sphere of practical politics
can point to his treatises on Economia Publica
(1859), and Ln Chiesa e lo State (1878).
MINIE Clatd Etienxe, inventor of the Minid
rifle, born in Paris in 1814, died in 1879. He en-
listed in the army as a private soldier, and quitted
it as colonel in 1858. He devoted his principal
thought to the perfecting of fire-arms, and in 1849
invented the 5Iinie rifle. In 1858 the khedive of
Egypt appointed him director of a small-arms
factory and musketry school in Cairo.
1084
MINING
MINING. See Britanniea, Vol. XVI, pp. 440— 472. The product of the world's mining for 1880 was :
Australia
Austria
Belgium
France
Germany
Gt. Britain and Ireland.
Italy
Russia
Spain
Spanish America
Sweden
United States
Otlier countries
The World ,
Value of a Year's Product.
$2,500,000
$.0,000,000
22,600,000
30,000,000
55,000.000
70,000,000
335,000,000
15,000,000
2,600,000
$70.000,000 j:081I.OUO,000 |3CO,000,000
$10,000,000
15,000,000
2,500,000
16,000,000
20,000,000
60,000,000
10,000,000
6,000,000
30,000,000
17,600,000
6,000,000
170,000,000
5,000,000
Number of Result
perllanr
$40,000,000
40,000,000
32,500,000
70,000,000
95,000,000
396,000,000
10,000,000
50,000,000
30,000,000
50,000,000
5,000,000
385.000,000
17,500,000
96,000
92,000
105,000
206,000
231,000
538,000
36,000
207,000
70,000
150,000
29,000
560.000
70,000
f42!.0O
430.0a
310.00
360.00
400.00
736.00
260.00
240.00
430.00
3a3.00
175.00
These returns of the world's mining are based on Mulhall's tables, and are for 1880.
In the following list we give the mineral products of the United States for 1887 and 1888. (From the latest report of the-
United States Geological Survey on the Mineral Production of the United States:)*
Metallic Pkoducts.
Pig iron, spot value long tons
Silver, coining value troy ounces
Gold, coining value '*
Copper, value at New York City lbs.
Lead, value at New Y'ork City short tons
Zinc, value at New York City "
Quicksilver, value at San Francisco flask£
Nickel, value at Philadelphia lbs.
Aluminium, contained in alloys
Antimony, value at San Francisco short tons
Platinum, value (crude) at New York City, troy ounces
Total value metallic products
Non-Metallic (spot values).
Bituminous coal long tons
Pennsylvania anthracite ^ "
Building stone
Lime barreli
Cement barrels
Salt "
Limestone for iron flux long tons
South Carolina phosphate rock "
Zinc-white short tons
Mineral waters gallons sold
Borax.
..lbs
Gypsum short tons
Manganese ore long tons
Mineral paints "
New Jersey Marls short ton
Pvrites long tons
Flint
Mica.
..lbs
Corundum short tons
Sulphur "
Precious stones
Crude barytes long tons
Gold quartz, souvenirs, jewelry, etc
Bromine
Feldspar long tons
Chrome iron ore "
Graphite Iba
Fluorspar short ton
Slate, ground as pigment long ton
Cobalt oxide lbs,
Novaculite "
Asphaltum short tons
Asbestus ; "
Rutlle lbs
Total value non-metallic mineral products
Total value metallic mineral products
Estimated value of mineral products unspecified.
Grand total $591,1
6,489,738
5,783,632
1,624,927
1.270,622
180,556
85,903
83,250
207,328
19,000
100
500
6,253,295
8,056,881
8,488.000
433,706
20,000
9,628,568
7,589,000
96,000
25,600
24,000
600.000
54.331
30.000
48,000
20,000
307,380
8,700
1,500
400,000
6.000
2,500
12.'2(;6
1,.'>00,000
5:^.800
100
1,000
$107,000,000
59,196,000
33,175,000
33,833,954
15,924.951
5,500,856
1,413.126
128.382
65,000
20,000
2,000
$256 ,'258,267
122,497,341
89,020,483
26,600,000
24,643,500
24,598,569
22,662,128
4.633,639
4,377,204
2,719.000
1.951,673
1,600.000
1,709,302
455,340
430.000
256.000
380,000
300,000
167,6.'i8
175.000
70.000
91,620
64.860
110,000
75,000
96,290
80.000
20,000
33,000
30,000
'25,000
18,441
18,000
331,500
3,000
3,000
328,914,528
256,'258,'267
6,000,000
6,417,148
41 .'269,240
1,596,500
184,670,624
160,700
50,340
33,826
205,656
6,992,744
7,831,962
6,377,000
480.568
18,000
8.259,609
11,000,000
95,000
34,6'24
20,000
600,000
52 ,.600
32.000
•70.500
600
3,000
16,000
199,087
10,200
8.00O
416,000
5,000
2,000
18.310
1. '200 .000
4.000
1,'iO
1,000
$121,926,800
.63,441,300.
33,100,000
21,052,440
14,463,000
4,782,300
1,429,000
133,200
74.905
16,600
1,838
98,004,666
84,552,181
25,000,000-
23,376,000
18,856,626
15,838,500
6,186,877
4,093,846
3,226,200
1,886,818
1,440,000
1,261,475
5SO.00O
4'25,00O.
333,844
310,000
300,000
210,000
185,000
142 ,'250
108 000
100,000-
88,600
75,000
75,000
61,717
56,100
40,000-
34,000
20,000
20,000
1S,774
16,000
16,000
4,500
3,000
'285.864,M2
•250,419,'288
6,000,000
$542,284,225
* The report ot the United States Geological Survey Office, of mineral productions In 1889, had not been completed wheos
this edition was ready for publication.
M I N I N G
1085
The following lists are taken from the eleventh census, as published in 1891. The Coal product of the
several States was :
Alabama
Georgia and North Carolina. . .
Illinois
ludiaoa
Kentucky
Maryland
Michigan
Ohio ;
Fennsylvania anthracite
Pennsylvania bituminous coal.
Tennessee
Virginia
West Virginia
9,976,7
45,544,S
36,174,(
1,925,(
$;',,787,426
:«9,382
1I,7»,203
2JS87,862
2,374 ,:«9
2,517,474
11.5,011
9,355,400
65,718.165
27,953,215
2,3:«,309
804,475
5,086,584
!!23,972
154,994
6,115.377
1,454,327
946,288
2,228,917
100,800
0,008,595
28.640,819
18,425,163
495,131
45,896
1,829,844
»476,9I1
232,005
8,779,832
2,150,258
1,134,960
2,685537
224,500
7,719,667
42.172,942
18,567,129
629,724
108.092
2,013,671
Coal Product We.st of the Mississippi River in 1889.
[The figures given are for the short ton of 2,000 pounds.]
Number of Miles.
Total
product.
Made into
coke.
Value of total
product at
mines.
Divisions and States
Regular
establish-
ments.
Country
Banks
and local
mines.
Average
price per
ton.
569
1,326
16.067,500
321,462
$24,413,262
$1.52
Trans-Mississippi Valley.
449
1,2:M
10.051,229
13,143
14,271,022
1.42
5
127
10
172
123
«
4
98
338
295
223'
356
16
6
91
30,307
2,280,763
752,832
4,061,704
2,567,823
279,584
128,216
4,8.30,368
46,^S1
3,291,7!)4
l,32:i.806
5,392,220
3,478,058
.395,836
340,617
7,486,004
1.53
1.48
1.76
1.83
1..35
1.42
500
12,618
•25
Texas
Rocky Mountain Region
308.319
1.55
Montana
8
15
53
18
4
22
22
10
40
12
7
1
363.301
1,388,947
2,360,536
486,983
2:36,601
1,179.903
30,576
8.11.623
1,748,618
3,605,622
872,785
377,456
2,655,636
269,526
6,000
2,217
1.53
1.79
1.60
2.25
New Mexico
Utah
Pacific toast
10
12
1
186,179
993,724
451,881
2,203,755
2.43
2.22
The total amount of coal produced in the States
and Territories west of the Mississippi River aggre-
gated in the calendar year :
Short tons.
1889 16,067.500
IWO 4,584,324
Increase 11,483,176
The value of this product at the mines was as
follows :
Increase 15,583,540
It is apparent, therefore, that the quantity of
coal produced in 1889 has increased to more than
threefold during the decade, while the value has
decreased from $1.93 per ton at the mines in 1880 to
.$1.52 in 1889.
Four States and Territories are now given as pro-
ducers of coal, for which no product was reported
2
in 1880 — namely, North Dakota, Texas, New Mexico,
and Indian Territory.
The Lead product of the United States in 1889
was as follows :
States and Territories.
Tons.
Value.
Total . .
130,903
$4,712,7.57.27
3,1.58
53
70,788
23,172
10,183
1,994
4,764
110
16,075
98,747.84
1,999.65
2,101,014.31
1,042,629.31
456575.40
72,653.64
170,754.59
4,653.44
763329.09
Idaho
rtah
\
1086
MINING
Tlie total product of the lead and zinc mines of the States east of the Rocky Mountains has been
ai^ follows ;
Total Product of the Lead and Zinc Mines East of the Rocky Mountains.
Total value.
• Zinc Ore.
Lead Ore.
Short tons.
Value.
Short tons.
Value.
Total
$4,804,179.24
234,503
$3,049,799.25
50,238
$1,754379.99
3,650.00
4.800.00
3,600.00
402,428.47
3,595,218.18
2,520.00
175,052.20
152,280.00
404,630.39
130
3,250.00
20
173
400.00
4,800.00
4.50
39,575
93,131
140
63,339
12,906
24,832
3.600,00
299,192.05
2,024,057.14
2,520.00
175,052 20
141.500.00
400,567.86
JP^^* •
3,617
44,482
103,236.42
,.- j
1,671,161.04
268
1,678
10,720.00
64,062.53
T"Tal Production of Precious Stones, Ornamental Min- | The production of Manganese from 1880 to 1891, Inclusive,
ERALS, etc., in THE UNITED STATES IN 1889. i Was aS follOWS :
Production of Manganese Ore in the United States.
$81,162
Sapphire
Emerald
Aquamarine
Phenacite
"lopaz
Turquoise
Tourmaline
Garnet
Quartz
Amethyst
Rose Quartz
Smoky Quartz
Gold quartz
liutilated quartz...
Dumortiente iu quartz
Quartz coated with
chalcedony
Chrysoprase
Agatized and jasperlzed
wood
Uanded and moss jas-
per
Amazon stone
Pvriie
C'hlorastrolite
Thomsonite
Kluorite
Fossil coral
Aztirite and malachite.
Catliuite (pipestone).
•Zircon
•Gadolinite, ferguson-
ite, etc
♦Monazlte
•Spodumcne
twooden ornaments
decorated with min-
erals
iMIscellaneous miner-
als
23,175
2,250
1.633
2,750
2,000
200
53,000
2,037
5,000
16,000
16,500
20,000
2,037
5,000
16,000
15 ,.500
20,000
♦Used to extract the rarer elements for chemical pur
poses.
tSuch IU) clocks, horseshoes, boxes, etc.
} For cabinets, museums, etc.
MINING
1087
In the following table will be found a statement
of the total production of Petroleum in the United
States in 1889, by States :
PennsylvanJa and New York.
Ohio
West Virginia
Colorado
California
Indiana
Kentucky
Illinois
Kansas
Texas
1,486,403
!,471,965
358.269
316,476
147,027
32,758
5,400
l,4fiO
500
In this statement the production of Pennsylvania
and New York is united. The Bradford (Pennsyl-
vania; and Allegany (New York) fields are re-
garded as one in petroleum reports. Of the 21,486,-
403 barrels produced in Pennsylvania and New
York in 1889, 7,158,362 barrels were produced in
these two districts. The Bradford district lies
partly in Pennsylvania and partly in New York.
The collection and shipment of its product by pipe
lines is such that it is almost impossible to separate
the quantity of oil produced in Pennsylvania from
that produced in New York.
Since pig-iron is directly made from iron ores,
and we have no recent statistics of the amount of
iron ore mined in this conntry, we insert here the
results of the Eleventh Census in the pig-iron in-
dustry instead.
The production of Pio-Iron during the year end-
ing June 30, 1890, was the largest in the history of
the iron industry of this country, amounting to
9,579,779 tons of 2,000 pounds, as compared with
'3,781,021 tons produced during the census year 1880
and 2,052,821 tons during the census year 1870.
From 1870 to 1880 the increase in production
amounted to 1,728,200 tons, or nearly 85 per cent.,
while from 1880 to 1890 the increase was 5,798,758
tons, or over 153 per cent. The following table
shows the production of pig-iron in the various sec-
tions of the country in the census years 1870, 1880,
and 1890, in tons of 2,000 pounds, including castings
made direct from the furnace. The statistics for
1870 and 1880 are for the census years ended May
31, but for 1890 they cover the year ended .June 30.
Tons of 2,000 Pounds.
Districts.
Year ended
May 81, 1870.
Year ended
May 31, 1880.
Year ended
June .30, 1890.
New England States.
Middle States
Southern States
Western States
34.471
1,311,649
184,540
522,161
30,957
2,401,093
350,4:^
995.:C5
3,200
33,781
5,216,591
1,780,909
2,522,351
26,147
Total
2,052,821
3,781,021
9,579,779
From the above it will be seen that the pig-iron
industry of New England has been practically
stationary during the past twenty years, while dur-
ing the same period, and especially since 1880,
there has been a wonderful development of the
manufacture of pig-iron in all other sections of the
country.
The following table gives the production of pig-
iron by States, in tons of 2,000 pounds, including
castings made direct from the furnace, during the
census years 1880 and 1890, with the number of com-
pleted furnace stacks at the close of each year, the
relative rank of each State and its percentage of
the total production.
States and
Territories.
Year Ended May :'.l. ISXO.
Rank
Complet 'd
furnace
stacks.
Production
of pig-iron
in tons.
Percentage
of total
production.
1
2
Pennsylvania...
269
103
57
20
27
14
10
17
11
15
22
22
21
10
8
4
31
6
1
1
1
1
1
7
2
1,930,311
518,712
313,368
157,414
119,.586
118,282
95,468
95,050
80,050
62,3.36
f)9,664
58,108
47,873
23,099
18,779
18,2.37
17,90li
9,!>43
.3,200
2,015
1,400
620
51.05
3
4
5
6
7
8
9
10
11
12
13
14
New York
New Jersey
Michigan
Wisconsin
Illinois
Missouri
West Virginia...
Alabama
Maryland
Kentucky
Tennessee
8.29
4.16
3.16
3.13
2.52
2.51
2.13
1.65
1.58
1.54
1.27
15
16
Connecticut ....
17
18
19
Virginia
Massachusetts ..
2.61
20
Maine .
21
22
23
Vermont
Minnesota
North Carolana .
Utah
24
25
Total
681
3,781,021
100 00
States.
Year Ended June 30, 1890.
Rank
Complet 'd
furnace
stacks.
Production
of pig-iron
in tons.
Percentage
of totlll
production.
1
2
Pennsylvania...
Ohio
224
71
48
15
37
31
19
26
10
18
5
8
14
6
5
8
2
2
4,712,511
1,302,299
890,432
674,506
359,040
302,447
290,747
224,908
210,0.37
145,040
108,764
99,131
96,246
44,199
36,747
21,700
12,949
11,470
8,950
8,411
8,381
4,787
3,700
3,377
49.19
3
4
Alabama
Illinois
9.29
5
6
7
8
9
10
11
12
13
14
15
16
17
18
New York
Virginia
Tennessee
Michigan
Wisconsin
New Jersey
West Virginia . .
Missouri
Maryland
Kentucky
Georgia
Connecticut
Colorado
3.76
3.16
3.04
2.35
2.19
1.51
1.14
1.04
1.00
19
20
21
22
23
24
25
Oregon
Massachusetts..
Washington
Maine
North Carolina.
Minnesota
Total
562
9,579,779
Quicksilver Mixing in the United States. —
During the calendar year 1889 there were 26,464
flasks, or 2,024,490 pounds, or 1.012 short tons of
quicksilver produced in California. About 20
flasks were produced in Oregon. The product is
notably less than the usual yield. In 1888, 33,250
flasks were produced.
1088
Itf I N I N G
The World's Production of Quicksilveu for
Ten Years.
■a .>,
Flasks.
119.168
120,933
115,221
115,119
101,828
98.354
103.061
108.787
109,914
101,236
1
■n 5-1 71 Ci -»■ uT ^ c r^ -J p)
•^ -r '^' ^ ff- -^ «■ t^ w ^ i^
■^ 51 0 -* :tc-. -Moots t*
1
i
Is
0
2II
<
Flasks.
10,510
11,333
11,663
13,152
13,967
13,503
14,496
14,676
14,962
15,295
a
<
Flasks.
45,322
44,989
46,716
49,177
48,008
45.813
61,199
.63,2
61.872
49,477
1
Total of all
mines. United
States.
Flasks.
59,926
60,851
52,732
46,725
31,913
32,073
29.981
33,760
33,250
26,464
£
1
f^
iiiiliilii
H
Tlie production of cut mica in the United States
in the census year amounted to 4f),.500 pounds, val-
ued at $50,000. In addition to this. 19(1 short tons of
scrap or waste mica were sold for grinding pur-
poses, with a value of $2,450. The production in
1880, as given in the Tenth Census report, was 81,-
()fi9 pounds of cut mica, valued at .$127,825.
A review of the annual production during the
past nine years sliows that the industry advanced
in importance until 1885. Since then the tendency
has been downward, though the fluctuations in the
production of the different regions have caused
much irregularity in the annual totals. The fol-
lowing talile does not include statistics of scrap and
wasle mica, as there had been no attempt prior to
18K!) lo determine the amount of this waste which
has been utilized :
Cut Mica Produced in the United States.
Years.
Amount
(Pounds).
Value.
18.S0 .
81,669
$127,825
100,000
250,0(HI
l.SSJ
100,000
250.000
1S.S:;
114,000
285,000
1S.SI
147,410
368.625
1,SK^.
92.000
161,000
18.sii
40,000
70,000
1 8.-^7
70,000
142,250
48,000
70,000
18.S'.l. ,
49,500
50,000
During the years 1883 and 1884, when mica min-
ing was in its most flourishing condition, the man-
ufacturers of stoves consumed probably 95 percent,
of the product, and the fancy grades and large
sizes of sheet mica which were then used found a
ready sale at highly prolitalile prices. Under this
stimulus of large profits many surface deposits or
pockets were opened by farmers, who worked them
occasionally when other business was dull and re-
alized a considerable profit on their production. As
long as the demand for large sizes continued, this
intermittent sort of mining could be carried on
with success, but when the fashion in stove panels
changed, and small sheets were used in place of
large ones, the demand for the latter fell off to a
great extent.
Production and Value of ^Ika in the United-
States in 1889.
Di^itvibution.
Cut.
Scrap.
Total
Pounds.
49,500
40,000
6,7000
2,800
Value.
$50,000
Short tons.
196
Value.
$2,450
New Hampsliire
40,000
7,000
3,000
160
2,000
Virgiuia and South
Dakota
36
450
Slate Mining in the United States. — The
total value of all slate produced in the T'nited
States in 1889. as sliown by the following table,
is $3,444,863. Of this amount, $2,775,271 is the
value of 828,990 squares of roofing slate, and $6(>9,-
592 is the value of slate for all other purposes be-
sides roofing.
As compared with the statements of the tenth
census report of 1880, the roofing slate product of
1889 is nearly twice as great in number of squares
and in value. A consideration of the slate used for
purposes other than roofing appears to have been
omitted from the Tenth Census report. The total
value of all slate produced in 1889 is more than
twice as great as that considered in the Tenth
Census.
According to "Mineral Resources of the United
States, 18S9," the total number of squares of roofing
slate produced in that year is 662,400, valued :it
$2,053,440.
Distribution of the Quarries. — Twelve States
at present produce slate. A line drawn on
to the map from Piscatacjuis county, Maine,
Polk county, Georgia, and approximately fol-
lowing the coast outline, passes through all the
important ^hlte-producinp localities. According
MINING
1089
to amount and value of product, the most impor-
tant States are, in the order named, Pennsj'lvania,
Vermont, Maine, New York, Maryland, and Vir-
ginia. In the remaining six States productive oper-
ations are of limited extent, and in the case of
Arkansas, California, and Utah, of very recent
date.
Copper Mining in the United St.\tes. — Since
the census year 1880 the United States has
risen to the rank of the largest copper producer in
the world, outstripping by far any other country.
During the decade Arizona and, later, Montana
have become important producing States, the latter
now acquiring and maintaining its rank as the
Production op Slate in the United States for the Year 1889.
States.
Number of
quarries.
Number of
squares of
roofing slate.
Total value of
roofing slate.
Total value of
slate for oth-
er purposes.
Total value of
all slate
produced.
I
2
4
4
5
1
5
16
104
1
60
3
60
2.504
3.050
43.500
23,100
3,000 .
2,700
17.167
474,602
(")
2.35,850
23,457
$240
13,889
14,850
214,000
105.745
15,000
10,800
85,726
1,636,945
(n)
592,997
85,079
(1)
(n>
$480
(a)
4,203
(n)
125
44,877
374,831
(a)
245,016
(«)
$240
13,889
15,330
214,000
110,008
15.000
10,925
130,603
2,011,776
(a)
838,013
85,079
California
i';«?'-s'a
Maryland
MichiRrtu
New Jersey .
New York
Pennsylvania.
Utah
Vermont.
Virfriuii.
206
828,990 $2,775,271
$669,592
$3,444,863
(<i) None.
Copper Production in 1889.
■ states and Territories.
Ore
produced
(Snort tons).
Mineral
(Pounds).
Black
copper
(Pounds).
Matte.
' Pounds.
Fine copper
contents
(Pounds).
3,322,742
117.804,926
39,713,237
159,547,390
220,569,438
Michigan
2,43.3,733
658.837
155,586
34,586
117,804,926
87,465,675
97,868,064
31,362,685
3.88;i,014
10,176.744
29,532.493
4,000
147,800,.i90
4.126.000
7.620. 8U&
leader. While by far the greater part of the metal
produced is ol)tained from ores carrying only the
leaser metal, important quantities in the aggregate
are derived from ores in which lead, gold and sil-
ver are the principal constituents of value. These
quantities are difficult to trace to their source. The
ores are purchased by lead and copper smelters in
the open market, often in small parcels, indirectly,
through sampling works. Sometimes copper is not
even present in the original ore in marketable
(juantity, and becomes a factor only when it ap-
pears in a concentrated form in the mattes of lead
smelters and refiners.
The copper product of the United States was as
follows, in pounds, in the calendar year 1889 :
Pounds.
Arizona 31,586,185
M ichigan 87,4.55,675
.Montana 98,222,444
New Mexico.... 3,686.1.'W
Colorado 1.170,053
Idaho 156.490
Nevada '. 26,420
Utah 65.467
California 151.505
Wyoming 100,000
Vermont 72,000
.Southern States 18,144
Lead smelters and refiners 3,345,442
Total 226,055,%2
These figures include the quantities of copper re-
ported as an incidental constituent of other ores.
The details of the copper mining of the principal
producing States during the year 1889 are given in
the following table, but does not include those
mines fairly to be considered as precious-metal
mines:
Gold and Silver Produced in the United
States. — The following estimate of the gold and
silver produced in the United States, since the dis-
covery of gold in California, is complied from the
official reports of the director of the United States
mint :
Y'ear.
Gold.
Silver.
Total.
1849
$40,000,000
$.50,000
$40,0.50,000
1.S.T0
.50,000.000
50.000
50.0.50.000
1851
55,000.000
.50.000
.55,0.50,000
1852
60.000,000
.50.000
60.a50.000
1853
65,000,000
.50,000
65.050,000
1854
60,000.000
.50,000
60.0.50,000
1855
55,000,000
.50,000
.55.0.50,000
1856
&5,000,000
50.000
,5.5.0.50,000
1857
55.000,0I«
.50.000
55.0.50,000
1858
50,000,000
.500.000
f)0 ..500.000
1859
50,000,000
100.000
.50.100,000
1860
46,000,000
1.50,000
46.1.50,000
1861
43,000,000
2,000.000
45.000.000
1862
.39,200,000
4,500.000
43.700,000
1863
40.000,000
S,.50(l.000
4.S..50O,00O
1864
46,100,000
11,000,000
57,100,000
]090
MINNEAPOLIS — MIRECOURT
Year.
Gold.
.Silver.
Total.
1865
53,22,5,000
11,2,50,000
64,475,000
1866
53,500,000
10,000,000
63,500,000
1807
51,725,000
13,500,000
05,225,000
1868
48,000,000
12,000,000
60,000,000
1869
49,500,000
12,000,000
61,500,000
1870
.50,000,000
16,000,000
06,000,000
1871
43,500,000
23,000,000
66,500,000
1872
36,(100,000
28,750,000
61,750,000
1873
36.0IX),000
36,750,000
71,750,000
1874
33,400,902
37,3W,594
70,815,490
1875
33,467 ,8u6
31,727,560
65,195,416
1876
S9,929,](i6
:«,783,016
7S,712,1.VJ
1877
46,897,390
39,793,573
86,690,963
1878
51,2U(i,360
45,281,385
96,487,745
1879
:-iS.!«9.S.'i8
40,812,132
79,7n,9!iO
1880
3fi,OU0.O0O
38,450,000
74,450,000
1881
34.70().(i00
43,000,000
77,700,000
1882
32,500,000
46,800,000
79,800.000
1883
:iU,(iU0.O0O
46,200,000
76,200,000
1884
39,800,000
48,800,000
79,600,000
1885
30,800,000
51,600,000
83,400,000
1886
35,000,000
51,000,000
86,000,000
1887
33,000,000
53,3.57,000
88,357,000
1888
33,175,000
59,195,000
92,.370,000
1889
32,800,000
64,646,000
97,446,000
The total value of the precious metals exported
from Alaska up to the present time approaches
$4,000,000, the annual production of gold dust and
bullion being now .$700,000. Within a radius of 100
miles from Juneau quartz mills have been estab-
lished, with an aggregate capacity of 500 stamps.
Of these, 240 stamps are employed at the well-
known Treadwell or Paris mine, on Douglas island,
capable of reducing 600 tons of ore per diem when
both steam and water power are utilized.
MINNEAPOLIS, a city of Minnesota, the metrop-
olis of the State, built on a broad plain overlooking
the Mississippi River and St. Anthony Falls, the
scenery being very picturesque. The celebrated
Minnehaha Falls are situated between Minneapolis
and St. Paul. Several important railroad lines
have their junctions at Jlinneapolis. This place
has some extensive grain elevators, large flour-
mills, and works for the manufacture of iron-ma-
chinery, engines, boilers, farm implements, furni-
ture, carriages, etc. Population in 1891, 164,738.
See Britannica, Vol. XVI, pp. 474—175.
MINNEAPOLIS, a city, the county-seat of Otta-
wa county, Kan., on Solomon River. It contains
saw and grist-mills, a carriage factory, a machine
shop, and foundry.
MINNEHAHA, a beautiful waterfall near Min-
neapolis, Minn, The Minnehaha River falls 60 feet
down a limestone precipice. The legend of a love-
lorn Indian girl leaping over the fall has been
utilized bv Longfellow in his poem Minnehalia.
MINONK, a city of Woodford county, 111.. 118
miles southwest of Cliicago. Mining and agricul-
ture are the principal occupations, and the city has
a steam mill, eight elevators, and coal mines.
MINOT, Gboroe Ricii.vRDS (1758-1802), an Amer-
ican jurist. He began the practice of law in Bos-
ton, Mass., and in 1771 Ijocame clerk of the Jlassa-
chusetts house of representatives. Inl792hew.as
made probate judge for the county of Suffolk, in
1790 chief justice of tlie court of common pleas, and
in 1800 judge of the municipal court of Boston.
.Judge Minot published Hixtoni of the iDsun-ri-tirm in
MdxMichiis.'lh in J7.W (1786), and ronll,ii.;iiinn of t lie
(Hutchinson's) History uf Mnnsachnneltx Jlni/ From
the year 17.iS, leith an Introductory Sketch of Events
from Itn Orlijlnal l^eltlntienl (1798).'
MINT, the common name of a number of fragrant
labiate phmts. See Britannica, Vol. XVI. p. 491 ;
Vol. XII. p. 289; Vol. XVIll, p. 517.
MINT, United States. For general article ot
Mints and Coinage, see Britannica, Vol. XVI, pp.
480-91. In the United States there are five mints —
at Philadelphia (since 1793), New Orleans (1885),
San Francisco (1854), Carson City, and Denver — all
under the charge of the Bureau of the Mint of the
United Stales Treasury Department, and presided
over by the Director of the Mint. Only the first
three are in active operation, the other two
are really assay offices; and at Philadelphia alone
all the authorized coins are struck. The United
States coins and their weights are as follows, those
marked with an asterisk having been discontinued :
Denonnnatiou ^Veightin
Gold.
Double eagle 616
Eagle 258
Half-eagle 129
Quarter-eagle 64'6
3-dollar piece — 77'4
Dollar 26-8
Silver.
Dollar. 412-5
Trade-dollar* 420
Half-dollar 192-9
Quarter-dollar 96-45
Denomination ^Veigh.in
20-cent* 77-16
Dime SS58
Half-dime* iy-2
3-cent* 11-51
Minor Coins.
6-cent (nickel) . 77-16
3-cent (nickel) 30
2-eent (bronze)* 96
Cent (copper)* 108
Cent ( nickel )* 72
Cent (bronze) 48
Half-cent (copper)* 84
The following table shows the total coinage of
the United States from the beginning up to and
including 1885, and also for each subsequent year to
and including the fiscal year closing June 30, 1890;
Gold.
Silver.
Minor Coin.
To 18S5
l.S.Sfl
J8S7
1888
1889
1890
$1,389,981,508
28,945,542
23,972,383
•28,346,170
25,543,910
22,021,748
* 434,224,610
32,086,709
35,191,081
;i4,lS6.095
31.515,.>iG
30,815,837
i 17,463.608
343,186
1,215.686
1,218,977
900,473
1.416,862
Toia!
$1,518,829,201
$ 606,909,878
.$ 22,504,782
MINUIT, or MiNNEWiT, Petek (1580-1641). a
Dutch colonist. He was boru in Wesel, Rhenish
Prussia, and for a time was deacon in the Walroon
church in his native town. He then removed to
Holland, and in 1625 was appointed by the Dulch
West India Company its director in New Nether-
lands, and was the first governor of the island. He
returned to Europe in 1632. and in 1637 set sail from
Gothenberg with a body of Swedish and Finnish
colonists. He ascended the Delaware River, and
planted his colony near the present city of Wil-
mington.
MINUTE MEN, in the American Revolution, the
militia who were prepared for service at a minute's
notice.
MIRACLES. See Britannica, Vol. II, pp. 188, 191 ;
Vol. X. pp. 804, 809; Vol. VIII, p. 141 ; Vol. 1, 127;
Vol. IV p. 754 ; Vol. XXIV, p. 664.
MIRAJ. a native state of India in the southern
Mahratta country. Population, 69,732. The capi-
tal, Jliraj, near the Kistna River, has a population
of 20,(il6.
MIR.\MAR, a palace standing on the rocky shore
of the .\driatic near Orignano, six miles north-west
of Trieste, llie home of the Arcliduke Maximilian,
afterwards Emperor of Mexieo.
MIRANDOLA, a town of northern Italy, nine-
teen milc>s by rail nortlieast of Modena. It has a
fine cMlhivIr:!) and an old castle. Population 3,0l"i9.
MlRIOCOt'UT, a lown in tlie department of Vos-
ges, 236 miles southeast of Paris with manufac-
tures of lace and musical instruments. Popula-
tion 5,341.
MIRFIELD — MISSISSIPPI
1091
MIKFIELD, a maiuifacluring town in the West
Riding of Yorkshire, three miles from Dewsbury,
and four and a half from Huddersiield. It has a
townhall, a parish church, and manufactories of
woolen cloths, carpets, blankets, etc. Population
11,508.
MISERERE, the name by which, in Catholic
usage, the Fiftieth Psalm of the Vulgate (5l8t in
Authorized Version) is commonly known. It is
one of the so-called "Penitential Psalms," which
are said after Lauds on the Fridays in Lent, except
Good Friday. It has been commonly understood
to have been composed by David in the depth of
his remorse for the double crime which the prophet
Nathan rebuked in the well-known parable (2 Sam.
xii). For an account of the celebrated J/isccert' of
Allegri, performed annually in the Sistine chapel,
see Britannica, Vol. I, p. 581.
JIISERERE, a small movable seat attached to
each of the stall-seats of the choir of mediaeval
The land areas in square miles and the popula-
tions of the several counties of the State in 1890
were as follows :
churches and chapels, etc. It is usually ornament-
ed with carved work, and is so shaped that when
the seat-proper is folded up it forms a small seat
at a higher level, sufficient to afiford some support
to a person resting upon it. Aged and infirm ec-
clesiastics were allowed to use these seats during
long services,
MISHAWAKA, a post-village and a railroad
junction of St. Joseph county, Ind., four miles east
of South Bend. Wagons, carriages, farm-tools,
windmills, furniture, brushes, woolen goods and
flour are made here. Population .S,369.
MISIONES, an Argentine territory, lies between
the Uruguay and the Parand, and is bounded on all
sides but the southwest by Brazil and Paraguay,
Area, 20,823 square miles; population, 30,000 —
though before the expulsion of the .Tesuits (1707) it
exceeded 100,000, There are three low mountain-
chains radiating from the center. The greater
portion of the surface is covered with forest, pro-
ducing building and dye-woods, oranges, medicinal
herbs, and the yerba mate. Maize is largely grown,
and sugar-cane to some extent; of late years sev-
eral sugar-houses have been erected. Capital,
MISSISSIPPI, State of. For general article on
Mississipi'i, see Britannica, Vol. XVI, pp, 518-524.
The United States census of 1890 reports the area
as 46,810 square miles, including 470 square miles of
water surface. Population, 1,289,600, an increase of
158,003 during the decade. Capital, Jackson, with a
population 016,041,
] Counties.
Areas.
Pop,
1890.
Pop,
1880.
400
•tso
700
750
436
876
600
615
520
406
452
660
420
500
760
.'J70
480
556
820
430
549
990
870
750
370
540
1,072
720
490
680
740
720
680
630
560
470
660
570
536
720
1.055
720
770
895
560
,')76
608
460
680
666
1,1 16
720
530
415
400
755
61:0
425
580
630
26,031
13,115
18,198
22,213
10,585
29,980
14,688
18,773
19,891
10,847
14.516
15,826
18,607
18,342
30,2,33
8,299
24,183
10,424
3,906
14,974
8,318
12,481
39,279
80,970
12,318
11.708
11.251
14,785
18,947
8,333
17,961
20,6,t3
29,661
12,318
14,803
20,040
16,869
17.912
27,047
27,321
9.5,32
26,042
30,730
14,459
11,146
16,625
27,338
17/!94
26,977
2,957
6,494
21,203
14,940
13,679
3,286
17,922
11,740
8,382
10,138
10,635
22,649
14,272
14,0(M
Attala
11,023
13,492
17,905
9,0,36
16,768
1 Choctaw
riniborne
Clarke
15,021
Clav
17,867
Copiah
27,552
5,998
De Soto
22,9S1
B'ranklin
9,729
3,194
12,071
Hancock
Harrison. „
I Hiuds
6.4.39
7,89f.
43,95S
27.164
10.663
.lackson
Jasper
Jefferson
Jones
Kemper
La/ayette ....
Lauderdale. ....
Lawrence
7.607
12,126
17,314
3,828
15,719
21,671
21,501
9,420
13,146
20,470
Leflore
Lincoln
10.246
28.24-1
25,86i
6.90:
Marshall
29,33(>
28.5!W
18,348
8,741
1S,4.%
Noxubee
Oktibbeha
29,874
15.978
28,3,52
3.427
Pike
J3 85h
li,],"*
1,407
]6,76-,i
10.845
6.306
8,008
Smith
8,088
9JXA
720
635
390
490
*S5
450
424
590
880
775
430
592
640
472
1,020
9,384
14, .361
19,253
12,957
9,302
12,1.58
15,606
a3,164
40,414
9,817
12,060
17.592
12,089
16,629
36,394
4,661
Tallahatchie
10,926
18,721
12,807
8,774
8,461
13,030
31,238
25 ,.367
Wilkinson
17,81.'.
10.087
Yalobusha
15,649
,33,8t.T
1092
MISSOURI
The full list of governors of the State of Mis-
sissippi, including the dates of their terms of ser-
vice, is as follows :
TEKIIITORIAL.
David Holmes 1817-19
George Poindexter . . . .1819-21
Walter Leake 1821-25
David Holmes 182.'>-27
Gfi-hard C. Brandou.. .1827-31
Abraham M. Scott 1831-a3
Hiram U. Buuuels 1833-3.5
Chark'S Lynch 1835-37
Alexander G. MeNutt..l837^1
Tilghmau M. Tucker.. .1841-43
Albert, (i. Brown 1843-48
Josei.h \V. Matthews. . .1848-50
John A. Quitman 1850-51
John J. Guiou 1851
John M. .S
James Whitfield 1851-52
Henrys. Foote 1852-54
John J. McKae. 1854-58
William McWillie 1858-60
John J.Pettus 1860-62
Jacob Thompson 1862-64
Charles Clarke 1864-65
William L. Sharkey. . . .1865-66
Benj. G. Humphrevs. . .1866-70
James L. Alcorn 1870-71
Ridgley C. Powers 1871-74
Adelbert Ames 1874-78
John M. Stone 1878-82
Robert Lowry 1882-90
tone, 1890-94.
The governor's salary is $4,000.
The population of the chief cities and towns
are as follows: Vicksbiirg, 13,298; Meridian. 10,889;
Is atches!, 10,101 ; Greenville, 6,655 ; Yazoo City, 5,247 ;
CciUinibus, 4,552; Aberdeen, 3,445; Watei; Valley,
2.S2S.
Abbreviated Historic Outline. — The Territory
of ^lississippi was first visited by white men (it
is believed) in 1839. In the spring of 1541 Fer-
nando de Soto, the first visitor, who had spent
about a year on the Yazoo Bottoms, reached the
Mississippi River. Over a century later (1673),
Joliet and Marquette, two French explorers,
passed down the Mississippi, touching at several
points in the territory. In 1682 De la Salle and
de Tonti visited the Natchez Indians. The first
colony proper was established by Il)erville, with
200 French immigrants, on the eastern shore of
Biloxi Bay. A French colony and a fortress were
estaljlished at Natchez about 1716 and named
Rosalia, in honor of the Countess of Pontchar-
train. Rosalia Fortress was assaulted and cap-
tured by the Indians in 1729, but was retaken in
1830. In 1763 Eastern Louisiana, including most
of the present State of Mississippi, was ceded by
France to Great Britain, and in 17.83 the whole
passed into the possession of the United States
under treaty stipulations. The territorial govern-
inen! was organized in 1798. In Mareii, 1817, Ala-
bama was set ofif from the Mississippi Territory,
and in December, 1817, Mississippi was admitted
into the Union as a State.
Priigress of population nf Mississippi by decades:
180(1. 8,8.50; 1810, 40,352; 1.S20, 75,4 IS; 1,830,136,621;
1840. 375,651; 1850, 60.5,948; 1,860,791,631; 1870,827,-
922; 1880, 1,131,597; 1.S90, 1,289,600.
For numerous addilimial items relating to Mis-
sissippi, see the article U.mteu States, in these
Revisions and Additions.
MISSOURI, St.stk 1)1'. For general article on
MissouKi, see Kritannica. Vol. XVI, pp. 524-27.
The United States census of 1.S9lt. reports the area
as 69,415 square miles, includinij 6,sii square miles of
water surface. Populalion, 2.679,l.si, an increase of
510,804 during I lie (leca<le. ('a|iilal,.refferson City,
with apopulatiou of 6,7:;2. Tlic iMi|iuhvtion of other
chief cities and towns was as follows: St. Louis,
4.50.245; Kansas City, i:'.2,4l(i; St. ,Insoph. .52,811;
Springfield, 21, ,842; Sedalia, 13,994 ; Hannibal, 12,SI6;
.Toplin, 9,909; Mdlierly, 8,21,'!; Carthage. 7,9(i2; In-
dependence, 6,373; Chillicothe, 5,099; Louisiana,
5.071; Trenton, .5011 ; Mexico, 4,789; Clinton, 4.689;
Warrensburg, 4.682; Ijexington, 4..538; Brooktield,
4,.534; Fulton. 4,2.S'.i; Cape lurardeau, 4,238 ; Mar-
shall, 4,258; Booneville, 4,132; Maryville, 4,017;
Columbia, 3,985; Carrollton, ,3,858; Kirks ville, 3,491;
Macon City, 3,350; Cameron, 2,,S95 ; Butler, 2,812;
Holden, 2,515.
The land area in square miles, and the popula-
tions of the several counties in the State of Mis-
souri in 1890, were as follows :
Adair
Andrew. .
Atchison.
Audrian
Barry
Barton. ..
Bates
Benton. .
Bollinger
Boone
Buchanan..
Butler ,
Caldwell..
Callaway..
Camdem..
.Cape Girardeau.
Carroll
Carter
Cedar . .
Chariton.
Christian .
Clark
Clay
Clinton .
Cole
Cooper —
Crawford .
Dade
Dallas
Daviess . .
DeKalb...
Dent
Douglas
Dunklin..
Franklin..
Gasconade.
Gentry
Greene
Grundy
Harrison.
Henry —
Hickory..
Holt
Howard..
Howell....
Iron
Jackson . . .
Jasper
Jefferson..
Johnson.
Knox
Laclede
Lafayette .
Lawrence
Lewis
Lincoln, , .
Linn
Livingston.
McDonald..
Macon . . .
Madison .
Maries .. .
Marlon.. .
Mercer . .
Miller
Mississippi ..
Moniteau . . ..
Monroe
Montgomery.
17,470
16,000
15,533
22,074
18.504
32,223
14.973
13,721
26.043
70,100
9,964
16,152
25.131
10.W0
22.0li0
25,742
5,799
23,301
15,620
26,254
14,017
15,126
19356
17,138
22,707
11,961
17,526
12.047
20,456
14,539
12,149
14,111
15,0.85
28,0.=)6
11,700
19,018
48,616
21,033
28.285
9.46:^
15,469
17,:«1
18.018
9.119
160,510
50,500
22,484
28.132
13,601
14,701
30,184
26,228
15.9&'>
18,346
24,121
20,668
11, 2K!
30,515
9,268
8,600
26,283
14,581
14,162
10,134
15.630
20.790
16,850
15.190
16,318
14,556
19,7.32
14,495
10,332
25,381
12,:i96
11,130
25,422
49,792
6,011
13,640
23.670
7,260
20,998
23,274
2.168
22,431
10,741
25.224
9,628
15,031
15,572
16,073
15,515
21,596
10.756
12,657
9,263
19.145
13,334
10.646
7,753
9,604
26,534
11453
17.176
28,801
15,185
20.304
23.906
7.387
15,609
18,428
8,814
28,172
liMi
11,524
25,710
17,583
15,925
17.426
20,016
10,196
7,816
26,222
8,876
7,304
24337
14,673
9,805
9.270
14,346
19,071
16,249
MISSOURI V A L L E Y — M I T C H E L L
1093
• Morgan
S'i;w Madrid.
Newton
Nodaway —
Oregon
Ozark
Pemiscot..
Perry
Pettis
Phelps..
Pike
Platte...
Polk
Pulaski .
Putnam...
F.alls
Randolph.
Ray
Reynolds .
Ripley
Saint Charles
Saint Clair
Saiute Genevieve .
Saint Francois
Saint Louis
Saint Louis city.
Saline.
Schuyler
Scotland
Scott
Shannon.
Shelby...
Sullivan .
Taney
Texas
Vernon,. .
VVarreu...
Washington,.
Wayne
Webster
Worth
Wright
Pop.
ISSlO,
Pop.
l.S»0.
12.311
9,317
-22,108
i!0,914
10,2.57
10,132
7.694
18,947
29,5!4
5,791
13.080
9,79.'>
. 5,970
li5,2i'.-
81,151
11,824
5,618
4.2!)9
11,895
27,271
12.(a:;
2ii;!:;i
]fi.2:!s
9,387
12..'>68
26,715
17,3* il!
15,734
7.250
I.-),3C5
12,294
M,S93
24.215
13,5.w
llj«»i
22,751
20,190
5,722
8,332
22,977
lti,747
9,883
17,347
5,377
23,065
14,125
10,390
13,822
;S6,307
451,770
:«,762
11,219
12,674
31.888
350,518
29.911
10,4(0
12,508
11,228
8,718
15,642
17,327
7,090
8,.t87
3,441
14,024
13,441
4,404
19,000
7,973
19,406
SI, .Wo
9,-J13
16,565
5,.599
13,206
19,.369
. 10,805
1.5.153
11,727
15.177
12,896
9,0Ui;
12,175
The full list of governors of the State, with their
dati? of service, is shown in the subjoined table :
.\l«.vander McNair.
Kryderick Bates..
.lolin Miller
Diiiiif!l Dunklin.. .
Lil'mrn N. Bosss..
Tlioni.w Uevnokls..
John C. Edwards..
.■\u3tiii A. King
Sterling Price
Truston Polk
iLi!icurk Johnson..
It. .M. Stewart
.1820-24
.1821-26 t
.1826-32 I
.18;«-36 '
1836-40
.1840-44
.1844-48
.1818-53
. 18.53-.57 '
....]S,V
.IS.".7
Claiborne F. .Jackson 1861
Muniilton K. (iiiuible. .1861-64
Thomas C. t'letoher 1865-09
Josupti W. McClurg 1869-71
Benj. Gratz Brown 1871-73
Silas Woodson 1873-75
Charles H. Hardin 187.5-77
John S. Phelps 1877-81
ThoniasT.Critteuden...l881-S5
JohnS.Murmaduke 88.5-187
Albert T. Morehouse. . .1887-S9
David R.Francis 1889-93
Governor Francis' term expires Jan. 10, 1893. The
governor's salary is ifo.OOO.
.\r.HRKVIATED HiSTOKIC RECORD OP MISSOURI. —
Territory first explored by De .Soto, in 1541-42; visi-
tcu by Marquette and followers in 1673. It formed
part of "Louisiana Hurc.hase,"a portion of which was
ors'inized as the District of Louisiana in 1805. The
tet ritory took the name of Missouri in 1812. In 1821
Missouri was admitted into the Union the "Missouri
Ooinpromise," by which compact it was provided
* that slavery should be forever excluded "from all
that part of Louisiana north of 36° .'50' latitude, ex-
ci'jit Mis!<ouri."
Progress of population of Missouri by decades :
1810, 20,845; 1820, 66,557; 18.30. 140,455; 1840,383,-
702: 1.850. 6,82,044; 1860, I.1.S2,012; 1.870. 1.721,295;
1880, 2,16s.::;,-;0: i.'^fti, 2.i;::i.ls.|.
For numerous additional items relating to Mis-
souri, see the article United States in these Re-
visions and Additions.
MISSOURI VALLEY, a post-village and a rail-
road junction of Harrison county, Iowa, situated
twenty-one miles north of Council Bluffs, onWillow
River.
MISTASSINI, Lake, in Labrador, some 300
miles north of Quebec, is strictly speaking an ex-
pansion of the River Rupert, which Hows into the
southern extremity of Hudson Bay. It is 100 miles
long from northeast to southwest by twelve in
average breadth.
MISTRAL, Frederick, a Provencal poet, born a
peasant's son near Maillaune, Sept. 8, 1830, and
studied law at Avignon ; but for law he had no lik-
ing, and went home to work on the land and to write
poetry. In 1859 he published the epic Mir'tio,
written in his native Pro^en^al dialect. This
charming representation of life in southern France
made Mistral's name famous throughout the coun-
try, and gained for him the poet's prize of the
French Academy and the cross of the Legion of
Honor. It also led to the formation of tlie society
called Lou Felibrige, which set itself to create a
modern Provencal literature. In 1807 IMistral
published a second epic, Calrndou, and in 1876 a
volume of poems entitled Lis Iselo d'Or, songs
steeped in the golden sunshine of the Mediterran-
ean and its vine-clad shores. Since then he has
written a novel, Nerto, and issued a dictionary of
the Provenr;al dialect, the preparation of which oc-
cupied him many years.
.MISTRETTA, a town of Sicily, near the north
coast, half-way between Palermo and Messina.
Population, 12,235.
MITCIIEL, John (1815-1875), an Irish patriot.
He practiced law for several years in Banbridge,
and then for a time was editor of the Dublin
"Nation." • In 1847 he founded the "United Irish-
man," and the following year was arrested for
treason. He was sentenced to fourteen years of
banishment, and sent to Tasmania, but escaped to
New York in 18.53. There he started the "Citizen,"
and advocated slavery, and later established the
"Irisli Citizen."' Subsequently he returned to Ire-
land, and was elected to Pariianient in 1874, but
5vas declared ineligible. The following year he
was again returned, but died l>efore any action was
taken in his case. lie published Life <»/ Hugh O'Niel,
Prince of Ulster (1845) ; The Last Conqtiest of Ireland
{Perhaps) 1861; History of Ireland from the Treaty of
Limerick (1868) ; and Life and Times of Aodh O'Neil,
Prince of Ulster (1868).
MITCJHELL. DoN.\i.D Grant, an American au-
thor, born in 1822. From 1841 to 1844 he worked
on a farm for the benefit of his health, and tlien
spent two years in Europe for the same purpose.
From that time his life has been given almost en-
tirely to literature. He has published Fresh Glean-
ings, or a New Sheaf from the Old Field of Continen-
tal Europe (1847); Tlie Battle Summer (1850); The
Reveries of a Bachelor (1851); Dream Life (1852); My
Farm at Edgenood (1863) ; Wet Days at Edgeieood
(1864) ; Doctor John (1866) ; Biiral Studies, with Xotes
for Country Places (1867); and About Old Story-
tellers (1875). Many of his books have been
written under the pen-name of "Ike Marvel."
MITCHELL. John Kearsle5' ( 1798-1858 ), an
American physician. From 1819 to 1822 he was a
ship-surgeon, and then settled in Philadelphia. In
1824 he became lecturer on the iiistitutPS of medi-
cine and physiology at the Philadelphia Medical
Institute, and in 1826 was made professor of chem-
istry. From 1.83.3 to M^U he held a similar position
in Franklin Institute, and then was chosen profes-
1091
M I T C H E L L — M 0 II A V E INDIANS
sor of the theory and pract ico of medicine in Jef-
ferson Medical College, in which capacity he served
until his death. He was the author of Saint Hele-
na, a poem, (1821); Indecision, a Tale of the Far
West, anil other Poems (1839) ; On the Wisdom, Good-
ness, and Power of God an Illustrated in the Properties
of Water (1834); On the CnipliKitimous Origin of Ma-
larious and Epidemic Fenrs (1S4;)) ; and Five Essays
on Varioi'f Chemical ami Mi ilnal Snhjects (1858).
MITCHELL, Maria (1SIS-1,S89), an American as-
tronomer. She studied under her father who was
an astronomer, and in 1847 she discovered a comet,
for which she received a gold medal from the King
of Denmark. In 1865 she became professor of as-
tronomy at Vassar College, which position she
held till her death. Miss Mitchell was the first
woman to be elected to the American academy of
arts and sciences.
MITCHELL, Samuel Weir, an American physi-
ologist, born in Philadelphia, Pa., Feb. 15, 1829. He
is celebrated for his researches on nerve-physiolo-
gy and the poison of serpents, and for his valuable
Smithsonian Contribution.
MITCHELL, Samuel Latham, an American natu-
ralist and physician, born at North Hempstead,
N. Y., Aug. 20. 1764, died in 1831. He was an
active promoter of the study of natural science, and
the author of several scientific works. He held
many important educational and legislative offices.
MITOHELL, a manufacturing town of Perth
county, Ont., thirty-two miles southeast of Goderich.
MITOHELL, a railroad junction and county-seat
of Davison county, S. Dak., situated on a branch
of the Dakota River. It is the seat of a Methodist
University.
MITCHELL, a post-village and a railroad junc-
tion of Lawrence county, Ind., situated 62 rnih tf
northwest of New Albany.
MITFORD, William, an English historian, bom
in London Feb. 10, 1744, died at Exbury, Feb. 8,
1827. He entered Queen's College, Oxford, but left
without a degree. In 1761 he succeeded to the
family estate of Exbury near the New Forest, and
in 1769 became a captain in the South Hampshire
militia, of which Gilibon was then major. By Gib-
bon's advice and encouragement he was induced to
undertake liis History of Greece. The author is an
intense hater of democracy, and can see in Philip
of Macedon nothing but a great statesman, in De-
mosthenes nothing but a noisy demagogue. Yet
his zeal urged him, for the very purpose of substan-
tiating his views, to search more minutely and
critically than his predecessors into certain por-
tions of Greek history, and the result was that
Mitford's work held the highest place in the
opinion of scholars until the appearance of Thirl-
wall and Grote. He sat in parliament from 1783 to
1818.
MITTWEIDA, a town of Saxony, 11 miles from
Chemnitz. It has an engineers' and a weavers'
school, and manufactures linen, woolen and cotton
goods. Population, 9,461.
MIVART, St. Geouoe, a distinguished naturalist,
born in England in 1827. He was educated for the
bar, but devoted himself to biological sciences. In
1862-84 he acted as professor of zoology and biology
at the Roman Catholic University College in Ken-
sington, and in 1890 was appointed to the chair of
philosopliy of natural history at Lovain. lie is
known as an able and zealous opponent of the
"Natural Selection" theory. Among his works are
The Genesis of Species; Man and Apes; Contemporarij
Evolution.; Lessons froia Xnlure; The Cat; Xatiire and
Thoui)lit, and The Origin of Unman Reason.
MIZEN, the sternmost of the masts in a three-
masted vessel.
MNEMOSYNE, in Greek mythology, the daugh-
ter of Uranus, and mother of the nine muses liy
Zeus. The principal seat of her worship was at
Eleutherw, in Bteotia.
MOBERLY, GEom:E, an English author and edu-
cator, born about 1803, died July 6, 1885. He was
long head-master of AVinchester School, and in 1869
became bishop of Salisbury. His writings were
mostly theological.
MOBERLY, a city and railroad center of Ran-
dolph county, Mo.. 148 miles west of St. Louis. It
contains the shops of the Wabash Western Rail-
road Company, flour and planing mills, and repair
shops for all kinds of machinery. Population in
1890, 8,215.
MOBILE, a city of Alabama. Population in
1890, 31,822. See Bri tannica, Vol. X YI, pp. 530^40.
MOCCASIN, the shoe of the North American In-
dian, made all of soft hide, and often ornamented.
The Moccasin Snake (Toximphis jiisclrorous) of
North America is a brown-colored poisonous swamp
snake; the skin is marked with black bars.
MOCK ORANGE, the name applied in England
to the Syringa, and in the United States to the
Prtirnis Caroliniana, a small evergreen resembling
the cherry-laurel.
MODESTO, a post-village, the county-seat of
Stanislaus county, Cal., 29 miles southeast of
Stockton.
MODJESKA. Helena, a Polish actress, born in
Cracow, Oct. 12, 1844. She began to act in a travel-
ing company in 1861 and four years later she made
a great name at Cracow, and from 1868 to 1876
was the first actress at Warsaw. Then she settled
with her second husl)and near Los Angeles, Cal., to
try farming; but the enterprise not succeeding,
she returned to the stage, and won a complete tri-
umph as Adrienne Lecouvreur at San Francisco in
1877, although she acted in English, of which lan-
guage she had known nothing seven months be-
fore. Since lliat time she has been acknowledged
one of the best of modern emotional actresses,
achieving her greatest triumph, both in the United
States and in Great Britain, in such roles as Juliet,
Rosalind, Beatrice, and in the Dame aux CamSHv.-
and Sardou's Odette.
MODOCS. See North American Indians, in thesn
Revisions and Additions.
MODULATION, in Mrsio. When in the course
of a melody the keynote is changed, and the orig-
inal scale altered by the introduction of a new sharp-
er flat, such change is called modulation. The art
of good modulation from one key to another con-
sists in the proper choice of intermediate chords.
Sudden transitions, without intermediate chords,
should be employed but sparingly.
MOFUSSIL (from an Arabic word meaning "sep-
arate") a term commonly used by Anglo-Indians
fur the rural part of a district as opposed to the
administrative headquarters. Thus in Bengal the
]\Iofussil means practically the whole province be-
yond the city Calcutta.
MOGUER. a town and small port of Spain, on
the Rio Tinto, near its mouth, and eight miles
east of Huelva, with some trade. Poi)ulation.
8.322.
.MOHAIR. See Britannica, Vol. XVI. p. 544.
MOHARRAINI, the first month of the Mohammc
dan year, kept by the Shiite I\Iohaninied;ins as a
month of feasting and mourning, in comniemora-
ti<m of the sufTerings of Hassan and Hussein,
nephews of the Prophet. A celebrated passion-play
is performed during this month in honor of the two
saints at several towns ;n Persia and India.
MOHAVE INDI.^NS. See Noinn American In-
unxs in these Revisions and Addiliims.
MOHAVE D E S E R T — M 0 M M S E N
1095
MOHAVE DBSERT, a basin, with little water or
vegetation, ehietly in the southeast of California,
and extending into Arizona. The Jlohave River
rises in the San Bernardino range, and finally dis-
appears in the ^Mohave Sink.
MOHAWKS. See North Americas I.vdi.ans in
these Itevislons and Additions.
MOHEG.\XS. See North American Indi.\xs in
these Revisions and Additions.
MOIIL, Hugo von, a German botanist, born at
Stuttgart in 1805, died at Tubingen in 1872. He
studied medicine at the University of Tiibingen,
and in 183.5 was made professor of botany there.
He was in his time the highest authority on veg-
etable anatomy and physiology. He published
Beitrdge zur Anatomie and Physlologie de.r Gewiichae;
Griindziige zur Anatomie and Physiologie der vegeta-
bilischen Zelle (1851) ; and Vermiachte Schriften.
MOIRE (from the French verb »io/nr. "to water,"
silk in a large pat tern, as distinguislied from tabiser,
to water or waive it in a small pattern), silks fig-
ured by the peculiar process called "watering."
They are wetted, and then folded with particular
care, to ensure the threads of the fabric lying all in
the same direction, and not crossing each other, ex-
cept as in the usual way of the web and the warp.
The folded pieces of silk are then submitted to an
enormous pressure, generally in a hydraulic ma-
chine. By this pressure the air is slowly expelled,
and in escaping draws the moisture into curious
waved lines, which leaves the permanent marking
called watering.
MOLESCHOTT, J.\kob, a Dutch physiologist,
born at Bois-le-Duc, Aug. 9, 1822. He studied med-
icine at Heidelberg, and taught there physiology,
anatomy and anthropology from 1847 until 1854,
when he resigned his chair, the senate of the uni-
versity liaving "warned" him on account of the
strong materialistic tendency of his writings. In
1853 he est;i))lished a private laboratory and worked
in it until IH.jfi, when he was nominated professor of
physiology at Ziirich ; in 1861 he moved to the uni-
versity of Turin, and in 1878 to that of Rome. He
has written Unlersuchnngcn zur Naturbhre des Men-
schen und der Tiere; Licht und Lcbcn; KUine Schrif-
ten. and other works.
MOLESWORTH, Mrs. .M.\kv Louis.i Stew.^kt,
novelist and popular writer for the young. She was
born of Scotch parentage at Rotterdam, and her
childhood was passed in Manchester and Scotland,
and partly in Switzerland. She began to write when
very young, and her first attempts were published
when she was only sixteen. Her first complete
works were written under the nam de phnne of Enuis
Graham, when she was about twenty-four. When
she was about thirty she began to write for chil-
dren and was at once successful, and has since held
foremost rank in this department. She has also
contributed largely to the better class of juvenile
magazines.
MOLESWORTH , Wii.lum N.a.ssau, an English
divine and historian, born at Southampton in 1816,
and died in 1877. He is best known by his valuable
History of England From the Year 1830. His brother
Guilford, born at Millbrook in 1828, is an eminent
civil engineer, and author of the popular Pocket-
book of Engineering Fonnube.
MOLINE, a city of Illinois. Population in 1890,
11,995. See Britannica, Vol. XVI, p. 631.
r MOLTKE, Helmcth, Coi-nt Von, field-marshal
of the German empire, born at Parchim. in Meck-
lenburg-Schwerin, Oct. 26, 1800, died April 24, 1891.
As chief of the general staff at Berlin ho planned
the Prussian campaign of 1866 against .\ustria, and
the German canipalgn of 1870-71 against France.
In 1812 he WM- ■••■"I I" <li<" miliiarv ai'iiileniv at
Copenhagen, where he remained under the strict-
est discipline for six years, and distinguished him-
self in the scientific branches of military study. In
1819 he became lieutenant in a Danish regiment,
but on the separation of Denmark from Norway he
determined to retire from the Danish and enter the
Prussian service. This change being effected, he
entered a Prussian regiment at Frankfort. His
parents having lost the whole of their property
from war and misfortune, he had to undergo many
hardships in order to maintain himself on the
slender pay of a Prussian officer, and at the same
time obtain instruction in foreign languages. In
1832 he was appointed to the staff, and for three
years he continued to develop by scientific and ex-
act study his extraordinary powers of combination
and organization. He obtained leave to travel,
and, arriving in Turkey at a critical moment, he
was entrusted by the sultan with the task of re-
modelling the Turkish army, and remained with
Mahmoud II. as military adviser till October, 1839,
when he returned to his old position at Berlin.
From 1858 to 1888 he was chief of the general staff
in Berlin, and he at once commenced the re-organi-
zation of the Prussian army. He elaborated plans
for the defense of the German coasts, and the crea-
tion of a German navy. His wonderful strategetical
power was displayed in the wars with Denmark in
186.3-4, with Austria in 1866, and with France in
1870-71, bringing them all to triumphant issues.
He married in 1845, Mary Burt, the daughter of an
English gentleman residing in Holstein, but had no
family, and his wife died in 1868. He mas a man of
great modesty and simplicity, and so reserved as
to have gained the popular epithet of TJie Sil'iit.
His ninetieth birthday v.as the occasion of numer-
ous honors at the hands of the emperor and the Ger-
man people. He was tlie author of several import-
ant works, of which the first. Litters from Turkey
and the Campaign in Turkey, were published in 1835,
and the Italian Cowpainn of 1S59 in 1868. The His-
tory of the German and French War of /570-7i, pub-
lished by the general staff in Berlin, was written
entirely under his direction, and the greater part
of it is actually from his pen. His Letters from
Russia, written in 1856 to his wife, were published
in 1877.
MOMIEN, a Chinese frontier town in the extreme
west of Yunnan. 135 miles northeast of Bhamo.
MOMMSEN. Christian Matthias Tiieodor. the
most learned historian of Rome, born at Garding,
in Sleswick, Nov. 30, 1817. He studied at Kiel, m-xt
spent three years traversing France and Italy in
the study of Roman inscriptions under commisi-ion
of the Berlin Academy, and in the autumn of 1.S48
was appointed to a chair of jurisprudence at Leip-
zig, of which two years later he was deprived for
the part he took in politics. In 18-52 he was ap-
pointed to the chair of Roman law at Ziirich, in
1854 at Breslau, and in 1858 to that of ancient liis-
tory at Berlin. Here he was engaged for many
years in editing the m.onumental Corpus Inscri])-
iionum Latinarum, and in 1873 he was elected per-
petual secretary of the academy. In 1882 he w as
tried for slandering Bismark in an election speech,
but was cleared both in the lower court and in
that of appeal. His fine library was burned in Ih.sO,
whereupon a number of English students presented
him with a collection of books to make good part
of his loss. Freeman characterizes Mommsen as
"the greatest scholar of our times, well-nigh the
greatest scholar of all times . . . language, law,
mythology, customs, antiquities, coins, inscriptions,
every source of knowledge of every kind — lie is
master of rhem all." Of his brothers, two have
achievt'd distinction; Tycho. ti^ni :ir Harding,
1096
M 0 M P 0 X — .AI 0 N S I G N 0 R
May 23, 1810, studied at Kiel, traversed Italy and
Greece, and held educational appointments at
Eisenach, Oldenburg, and Frankfort-on-Main until
his retirement in 1885. August, born at Oldesloe,
July 25, 1821, studied at Kiel, and taught in schools
at Hamburg, Parchim, and Sleswick. Most of his
works belong to the field of Greek and Roman
chronology.
MOMPOX, or MoMfos, a town of Bolivar in Co-
lombia, on the Magdalena, 110 miles southeast of
Cartagena. Founded in 1538; it contains a good
secondary school and a distillery. Population,
8,000.
MONACO. For general article on this small
principality see Britannica, Vol. XVI, pp. 717-718.
The latest accredited reports place the area at
eight square miles; population (in 1890), 12,000, of
whom 3,292 were in the town of Monaco, 6,218 in
Coudamine, and 3,794 in Monte Carlo. The capital
is under French protection. Prince Albert (born
in 18-18, succeeded his father. Prince Charles III.
Sept. 10, 1889), the present sovereign, has one son,
Louis, by a marriage, dissolved in 1880, with Lady
Mary Hamilton.* About 1,000 of the inhabitants
are employed in the rooms and gardens of the cele-
brated Casino. These gambling-rooms, built at
Monte Carlo on ground leased from the Prince of
Monaco, 1)p1i>h'.j to a joint stock company, and have
about 400,000 visitors. The climate of Monaco is
milder than ihat of any otiier place in the Riviera;
palms and aloes grow most luxuriantly, and rare
wild-Huwers are found on its rocky promontory.
See Metivier, Moiinco el si:i Prirces (2d ed. 1865), and
Boyer de Sainte- Suzanne, La Princirpautf, de Monaco
(1884).
MONA P.\S.SAGE, a water-way for vessels be-
tween San Domingo and Porto Rico. On the west
end of Porlo Rico is Mayaguez Harbor opening di-
rectly out upon the Mona Passage. The water at
the landing is not deep enough for vessels of large
draft, and for them the anchorage is about a half
mile from shore.
MoNA Island is a small, desolate, but beautiful
island lying about the middle of the M<ina Passage.
MONCALIKKI, a (own of Italy, on the Po, five
miles south of Turin, with a royal palace (1470).
Population, 3,403.
*The miirrin^o wiis deiilnrcd dissolved by the Pope of
Rome, Jan. ■". KKO. .-iiid I);- tbe .■ciKii'ngt prince, July 28, 1S,S0.
'MONCKTOX, Robert, a British general, gov-
ernor of Xew York in 17(52, and lieutenant-general
in 1770. He died in 1782.
MONCONTOUR, a village in the French depart-
ment of Vienne, 48 mile.s from Tours. It was tla-
scene of the defeat of the Huguenots under Coligny
by the troops of the King of France, Oct. 3, 1509.
MONEY. See Britannica, Vol. XVI, pp. 720-
738.
MONITOR. See Navy, in these Revisions and
Additions.
MONK, Maria (1817-50), a woman of bad charac-
ter who pretended in 1835 to have escaped from the
Hotel Dieu nunnery at Montreal, and who, coming
to New York, found a good many credulous adher-
ents, and published Aifful Disclu.'<uirs and Furthrr
Disclosiun;t, which had an enormous sale.
MONMOUTH, a city, the county-seat of AVarren
county. 111., 179 miles by rail west-southwest of
Chicago. It is the seat of Monmouth College
(United Presbyterian, 1856), with about 400 stu-
dents, and manufactures agricultural implements,
sewer pipes and cigars. Population in 1890, 5,837.
MONGX'IOUS, a term introduced by Linnaeus to
those plants which have the stamens and pistil in
different flowers, but on the same plant. Such
plants formed one of the classes of the Linnean
system, but were obviously a specially artificial
alliance, since that partial or complete separation
of the sexes to which we apply the terms monre-
eious or dioecious respectively arises continually
among the most unrelated plants or animals.
MONOGRAM, a character composed of two or
more letters of the alphabet, often interlaced M-ith
other lines, and used as a cipher or abbreviation of
;i name. A perfect monogram is one in which all
till- litters of the word are to be traced.
:\t(_)NOGRAPH, a work in which a particular sub-
ject in any science is treated by itself, and forms
the whole subject of the work — "an all-sided and
exhaustive study of a special or limited subject."
as it has been called. ^Monographs have con-
tributed much to our knowledge, especially in the
department of the natural sciences. The term,
liowever, is often loosely used for a small book on
niisrollaneous topics.
JIONONGAHELA, a river which rises in AVest
' irginia and flows north to Pittsburgh, where it
unites will) the Allegheny to form the Ohio.
i\l ( )NONG A 11 ELA CITY, a post-borough of Wash-
ington county. Pa., 21 miles south of Pittsburgh. It
contains a strawlioard paper-mill, planing-mills,
nianilla paper-mill, and gas works. Thrrearecoal-
mines in the vicinity. Population 4,086.
MONROE, a city, the capital of Ouachita
parish, in the nortl}ern part of Louisiana oa: Ouachita
River. Pojiulation, 3,251.
MONROE, a post-village, the county-seat of
Union county, N. C. in the southern part of the
State, near a'branch of the Yadkin River. It man-
ufactures carri.'iges.
MONROE, a post-village, the county-seat of
(ireen county. Wis., on a branch of the (!hicago,
Milwaukee & St. Paul Railroad. It has a foundry
and wagon factories. Population 3,865.
MONROE DOCTRINE. See Britannica, VoL
XIII, p. 192; Vol. XVI, p. 761 ; VoL XXIII, p. 762.
MONROEVILLE, a jiost-village and a railroad
center of Huron counly. Ohio, sixty miles west of
Cleveland. It has grain warehouses, and manu-
factures flour, beer and woolen goods.
MONSIGNOR, a title of honor given to prelates
of the Roman Catholic t!hurch. Formerly in France
the corresponding title of Moiiseitjiirur was allowed
to all high dignitaries of the church, to the prin-
ces of the blood royal, to the higher nobles, and
M 0 N S T R A N C E — .M 0 N T C E N I S
1097
to tlie presidents of the superior law-courts. But
from tlie time of Louis XIV. Monseigneur without
further addition was appropriated as the title of the
Dauphin.
MONSTRANCE, the sa-
cred utensil employed in
the Catholic Church for
the purpose of presenting
the consecrated host for
the adoration of the people,
as well while it is carried
in procession as when it is
exposed upon the altar on
occasions of special solem-
nity and prayer. It con-
sists of two parts, the foot or
stand upon which it rests,
and the repository or case
in which the host is exhib-
ited. The latter contains a
small semi-circular holder
called the lunula, or cres-
cent, in which the host is
fixed. It is commonly in
the form of a star or sun
with rays, the central por-
tion of which is of glass or
crystal, and serves to per-
mit the host to be seen.
MONTAGl'E, a village of Muskegon county,
Mich., situated on White Lake, five miles east of
Lake Michigan. It is a commercial town and is
especially noted as a shipping point for peaches.
:M0NTCLAIR, a post-village and a railroad cen-
ter of Essex county, N. J„ situated fourteen miles
northwest of New York.
MONTALCINO, a cathedral city of central Italy.
It stands on a hill (1900 feet), twenty-two miles
southeast of Siena. Population, 2.353.
MONTALEMBERT, M.\rc Re.vk, Marquis de, a
French military engineer, grand-father of the ora-
tor and statesman, born at Angoul^me in 1714, died
in 1800. He was the author of La Fortification Per-
pendiculaire, and the originator of the modern
application of the casemate to forts and bat-
teries.
MONTANA, State of. For general article on
MoNT.v.\.\, see Britannica, Vol. XVI. pp. 772-774.
The United States census of 1890 reported the area
and population of Montana as follows ; Area, 146,-
080 square miles. Population, 1.12.1.59. a gain dur-
ing the decade of 93,000. Capital, Helena, with a
population of 13,834. Population of Butte City,
10,701.
The full list of governors of Montana with the
dates of their official service, is as follows :
MoQstraDce.
Sidney Eserton iSM-m
Francis Meagher 186.5-4i6
Green Clav Smith. ... 1866-69
James M. .Uhlev 18<i9-70
Benjamin F, Potts .. 1870-82
J. Schuyler 1882-84
B. Piatt Carpenter . 1884-85
Samuel T. Houser 1885-86
Preston H. Leslie 1886-89
Joseph K. Toole 1889-98
Governor Toole's term expires Jan. 3, 1893. Sal-
ary of governor $2,600.
Abbrevi.\ted Historic OL-TLiNE of Moxt.\na. — The
part of Montana lying east of the Rocky Mountains
was included in the "Louisiana Purchase ;" that part
lying to the west was formerly included in Oregon
and Washington, The Territory of Montana was
first visited by the French in 1 742-43, also by Lewis
and Clarke in 1804-06. Gold was discovered in
1861; and mining began in earnest in 1862. The
Territory was organized in 1864, and was admitted
into the Union as a State Nov. 8, 1889.
Progress of population of Jlontana by decades :
1870, 20,595; 1880, 39,159; 1890, 132,159.
For nuiirerous additional items relating to Mon-
tana, see the article United States, in these Re-
visions and Additions.
In the absence of the reports of the official cen-
sus of the chief towns of the State, (not yet
published) the following estimates made for 1.S89,
by E. L. Lomax, have been kindly furnished by the
passenger department of the Union Pacific Rail-
road:
Anaconda
Great Falls
Ph illipsburi; in-
cluding Granite
and Rurasiy ....
Bozeman
Missoula
Livingston
Dillon
Deer Lodge ...
Billings
Miles City....'
Boulder
Marysville
White S n 1 ph nr
Springs
Fort Benton . ..
Stevensvillc...
Lewisiown
Corvallis
Elkhorn
(Jlendive
Maiden
Virginia
Victor
Sheridan
(Jlendale
Thompson Falls
Pop.
4.001)
3.730
S.a00
S.OOO
2..')00
•>,-2.Vt
2.000
1.600
l.iOO
1.400
l.iW
1.200
1.150
1.100
1.050
1,000
1.000
l.OfK)
1,000
1,000
1,000
Wickcs
Townscnd
Castle
Bonucr
Carroll
I Choteau
Kmpire
(irantsdale
Frenchtown . . .
Forsvtli
Sulesville
Fort Maginnis.
J:iy Gould
Ashley
Toston
Augusta
P:>rl.- City
Biir Timbers...
Cottonwood . . .
Ba.=iu
Jefferson
Twin Bridges..
Florence
New Chicago .
Cascade
Chestnut
Sun Kiver
Pop.
The land areas, and populations of the counties,
severally, of the State of Montana in 1890 were as
follows :
Beaver Head
Cascade
Choteau
Custer
Dawson
Deer Lodge
Fergus
Gallatin
Jefferson
Lewis and Clarke
Madison
Meagher
Missoula
Park
Silver Bow
Yellowstone
27.280
26..5K0
26.660
5.085
6.762
2,2"J5
1.3S0
26.00
4.2.W
4.6.T5
8,755
4,741
5,S08
2,056
15.155
3,514
6.246
6.026
19.145
4.692
4.749
14.427
6,881
23,744
2.065
Pop.
».64S
a.461
6,521
3,015
2,743
2.537
MONTBRISON, a French town in the depart-
ment of Loire, 35 miles southwest of Lyons, with
mineral wells and some ribbon manufacture. Pop-
ulation, 6,235.
MONTCALM, Locis de. Marquis, a French gen-
eral, born at Nismes in 1712, killed at Quebec in
1759. See Britannica, Vol. XX, p. 167 ; Vol. XXIII,
p. 735 : Vol. XXIV, p. 6.30.
MONT CENIS, or Monte Cenisio, an Alpine
peak and pass between Savoy and Piedmont.
Height of the mountain, 11,792 feet; of the pass.
6,884 feet. Over the pass a road was constructed
(1802-10) by Fabbroni, under Napoleon's orders, at
an expense of $1,500,000. Thirteen miles west of
the pass a railway tunnel, seven and a half miles
long, was begun in 1857 on the Italian side, and in
1863 on the French side, and was finished in 1870 at
iOOS
M 0 N T -DE- M A II 8 A N — M O N T E U U S A
a cost of $15,000,000. Through this tunnel passes
one of tlie inuiii continontiil overland routes from
London via I'aris to Brindisi, for Asia, Australia
and East Africa.
MONT-DK-MARSAN, the capital of the French
department of Landes, at the confluence of the
Midou and Douze, 92 miles by rail south of Bor-
deaux. It lias a mineral spring and manufactories
of chemicals, iron, etc. Population, 10,714.
MONTE OATINI, a watering-place of Italy, 30
miles northwest of Florence. Its mineral springs
are efflcacious for abdominal complaints, scrofula
and dysentery. The season lasts from May to Sep-
tember. Near here the Florentines were defeated
by the Pisans in 1315.
MONTEFIOKE, Sir Moses (1784-1885), an Eng-
lish Jewish philanthropist, descendant of a family
of bankers, born in Leghorn, Oct. 24, 1784, where
his parents happened to be sojourning. His grand-
parents had emigrated from Leghorn to London in
1750. In 1812 he married Judith Cohen, a lady who
went hand in hand with him in all his schemes of
philanthropy. As a stock-broker he achieved great
success. In 1818 he was elected president of the
Spanish and Portuguese community. From 1829
onwards he took part in the struggle for removing
the civil disabilities of English Jews.
In 1835 he was one of the parties to the contract
for the $75,000,000 given as compensation to the
slave-owners. He was for a time high-sheriff of
Kent, and, after long exclusion and repeated re-
election, was legally admitted as sheriff of London
in 1837. In that year he was knighted, and in 1846
was raised to a baronetcy. He distinguished him-
self by his sympathy with his countrymen in
various parts of the East. He made seven journeys
to the East, chiefly for the amelioration of the con-
dition of his countrymen. At Bucharest, during an
anti-Jewish ferment, he boldly faced the mob at
the risk of his life. He was presented with the
freedom of the City of London in 1873, and an ad-
dress in 1883. In memory of his wife he endowed
a .fswish college at Ramsgate in 1865. In his hun-
dredth year he was still hale and well, but died
July 29, 1885.
MONTEGUT, EwrLB, a French critic, born at
Limoges, June 24, 1826, and early made a reputa-
tion by a series of brilliant studies on English lit-
erature. He contributed to various journals, and
has published books of travel, a study of Marshal
Davout, and translations of Shakespeare, Macau-
lay and Emerson. Books of altogether exceptional
value in their critical insight are PoHes et Artistes
<Ie I' Italic; Tyi/es Litteraires, et Fantaisies EsthStiques;
Eniaia sur la Litterature Anglaise; Nos Marts contem-
porains; Les Ecrivains modernes de I'Angleterre;
Livrea el Ames des Pays d'Orient; Melanges critiques,
and Dramat7irges et Romanciers.
MONTENEilRO. For general article on Mon-
tenegro, see Britannica, Vol. XVI, pp. 779-81. The
latest authorized figures report the area at 3,630
square miles. The total population was stated in
official returns to number 220,000 in 1879 ; a later
estimate makes it 236,000, The capital is Oettinje,
with 1,.500 population ; Podgoritza, 6.000 ; Dulcigno,
5.000; Nisksic, 3,000; Dan i log rad, 1,000. The popula-
tion is mainly pastoral and agricultural. The Mon-
tenegrins belong almost entirely to the Servian
branch of the Slav race.
The constitution of the country, dating from
1852, with changes effected in 1855 and 1879, is nom-
inally that of a limited monarchy, resting on a
patriarchal foundation. The executive authority
rests with the reigning prince, while the legisla-
tive power is vested according to an "Administra-
tive Statute" proclaimed March 21, 1879, in a state
council of eight xnembers, one-half of them being
nominated by the prince, and the other elected by
the male inhabitants who are bearing, or have
borne, arms. Practically, all depends on the abso-
lute will of the prince. The inhabitants are divided
into 40 tribes, each governed by elected "elders."
and a chief or captain of district called Knjez, who
acts as magistrate in peace and as commander in
war. By the "Administrative Statute" of 1879,
the country was divided into 80 districts and six
military commands.
Reigning Prince and Royal Family. — Nicholas
I., Petrovic Njegos, was born October 7 (September
25), 1841. He was educated at Trieste and Paris,
proclaimed Prince of Montenegro, as successor of
his uncle, Danilo I., August 14, 1860. He was mar-
ried, Kovember 8, 1860, to MUena PHrorna Vuco-
lii ova, born May 3, 1847, daughter of Peter Vukotic,
senator, and vice-president of the council of
slate. Offspring of the union are six daughters
and three sons, Dcmilo Alexander, heir-apparent,
born June 29, 1871 ; Mirko, born April 17, 1879 ; Pner,
born in 1889.
Prince Kicholas's nominal yearly income is fixed
for the present at 9,000 ducats, or 4,100?. A yearly
sum of 48,000 roubles, or 4,800/., has been received
by Montenegro from Russia since the Crimean war,
as a reward for its friendly altitude during that
period. The Austrian governnit nt is stated to con-
tribute about 30,000 florins per annum towards
the construction of carriage roads in Monte-
negro.
Finances and Defense. — No oflScial returns are
published regarding the public revenue and ex-
penditure. Reliable estimates state the former at
600,000 Austrian fioriiis, or 60,000/. A loan of 1,000,-
000 florins was raised in Vienna in 1881 at an inter-
est of 6J-0 per cent, on the salt monopoly of the
jjrincipality, and 70,000/. is owed to Russia for grain
supplied in 1879.
The number of men capable of bearing arms, be-
tv een the ages of 17 and 60, is calculated at about
20,000. There exists no standing army, but all the
inhabitants, not physically unfitted, are trained as
Bt'ldiers, and liable to be called under arms. Re-
cently the Moslem inhabitants of Dulcigno have
been exempted from military service on payment
of a capitation tax.
The infantry are armed with the Russian Werndl
rifle, of which 25,000 have been distributed, and the
long ll-millimttre Gasser revolver. The artillery
consists of 24 9-centimt'tre Krnpp field pieces, and
24 mountain guns. By the Berlin treaty Montene-
gro is precluded from owning vessels of war.
Schools for elementary education are supported
by government ; education is compulsory and free ;
there were in 1889, 70 elementary schools, with
3,000 male and 300 female pupils. All males under
the age of 25 years are supposed to be able to read
and write. There is a theological seminary and a
gymnasium or college for boys at CettinjI, and a
girls' high-school maintained at the charge of the
Empress of Russia.
MONTENOTTE,asmall village of northern Italy,
twenty-six miles west of Genoa, where Napoleon
won his first victory over the Austrians, April 12,
1786.
MONTEPULCIANO, a town of Italy, a bishop's
see, situated on a high hill, forty-three miles from
Siena. It was the birth place of Politian and
Belarmine, and is famous for its red wine. Popula-
tion. 2.952.
MONTK ROSA, an Alpine mountain mass with
four principal peaks, in the Pennine ridge which
separates the Swiss canton of Valais from Italy.
The highest peak, the Dufourspitze, 15,217 feet
M 0 X T E S A N 0 — M 0 0 R E
1099
liigh, is extremely difficult of ascent, and was
first climbed by .Ur. Smyth in 1855.
MONTESAXO, a post-village, the county-seat of
Chehalis county, Washington, sixty miles south-
west of Olympia, on the south bank of the Chehalis
River.
MONTEVIDEO, a post-village, the county-seat
of Chippewa county, Minn., situated at the mouth
of the Chippewa, where it enters the Minnesota
River.
MONTEZ, Lola, adventuress, was born about
1S18 at Limerick, died at Astoria, L. I., Jan. 17,
1S51. She was christened Marie Dolores Eliza Ros-
aiina, her father being an English Gilbert, and her
mother of Spanish descent. Taken out to India, she
there lost her father by cholera; and, her mother
having re-married, Lola was sent home in 1826 to
Europe, and brought up at Montrose.in Paris, and at
Bath. To escape the match.arranged by her mother,
with a gouty old judge, she eloped with a Captain
James, whom in July 1837, she married at Xeath ;
hut the marriage ended in a separation and in her
return from India. She now turned dancer, and
after visits to Dresden, Berlin, Warsaw, St. Peters-
burg, and Paris, she came to Munich. There she
soon won an ascendency over the eccentric artist-
king, Louis I., who created her countess of Lands-
fe!d, and allowed her $25,000 a year. For more than
a twelvemonth she was all-powerful, her power di-
rected in favor of Liberalism and against the Jes-
uits; but the revolution of 1848 sent her once more
adrift on the world. Again she married, and, after
t )uring through the States and Australia, and after
two more "marriages" in California, in 1858 she de-
livered in Xew York a series of lectures written for
her by C. Chauncey Burr. She died, a penitent,
her last four months being devoted to ministering
in a Magdalen asylum near New York, and was
buried in Greenwood cemetery.
MONTGOMERY, Florence Sophi.4, a popular
writer of books for children, is the daughter of Sir
..\lexander Leslie Montgomery, Bart., of the Hall,
County Donegal, Ireland. Her first book, A Very
Simple Story, was warmly praised. Of its succes-
sors the chief are the widely popular Misunder-
stood; The Town Crier; Peggxi,and Other Tales, and
The Blue Veil.
MONTGOMERY, Rich.\rd. See Britannica, Vol.
XNIII. p. 790.
MONTGOMERY, Robert (1807-1885), an English
lioet, born at Bath in 1807, the son of one Gomery,
a famous clown. In 1830 he entered Lincoln Col-
lege, Oxford; in 1833 took his B. A. with a fourth
class; in 1835 was ordained, and was minister of
Percy Street Chapel, London, until his death at
iSrighton, Dec. 3, 1855. Of his 31 works in verse and
prose, two — Tlie Onxnipresence of the Deity and Satan
— are still remembered by Macaulay's onslaught in
the Edinburgh "Review."
MONTGOMERY, a city of Alabama. Popula-
tion in 1890, 21,790. See Britannica, Vol. XVI, p.
790.
MONTGOMERY CITY, a post-\nllage of Mont-
gomery county. Mo., 82 miles west of St. Louis.
Farming and dairying are the chief occupations.
The place contains a college, mill and manu-
factory.
MONTI, ViNCENZo (1753-1828), an Italian poet of
the classical school, remarkable for his political
tergiversation, anti-French, Napoleonist, pro-Aus-
trian in turn. He was professor at Pavia, and,
under Napoleon, state histiographer. His transla-
tion of the Iliad is admirable.
MONTICELLO, a city, the county-seat of Piatt
county. 111. It contains a steam-elevator and
flour-mill.
MONTICELLO.a post-village, a railroad junction,
and the county-seat of White county, Ind., 21 miles
west of Logansport. It has manufactories of paper,
furniture and woolen goods.
MONTICELLO, a city and railroad junction of
Jones county, in the eastern part of Iowa.
MONTJOIE ST. DENIS, the French war-cry. old
at least as Wace's day (12th century), from the hill
near Paris on which St. Denis underwent the joy of
martyrdom.
MONTMEDY, a town and fortress in the French
department of Meuse, 25 miles north of Verdun and
31 miles southeast of Sedan. It consists of two
portions, the citadel and upper town overlooking
the lower town, which lies in the valley of the
Chiers, a tributary of the Meuse. Built and forti-
fied in 1235, it was taken by the French in 1542,
1555, 1596 and 1657, and they, after it was definitely
assigned to them by the peace of the Pyrenees
(1659), had it re-constructed and re-fortified by
Vauban. It was captured by the Germans in 1815
and again in 1870. Population, 2.740.
MONTROSE, a post-borough, the county-seat of
Susquehanna county. Pa., eight miles from Mont-
rose Station. It is healthfully situated among the
high hills and is a pleasant summer resort.
MONTROSS, a post-village, the county-seat of
Westmoreland county, Va., situated 52 miles south-
east of Fredericksburg.
MONTYON PRIZES, rewards for single instances
of disinterested goodness discovered throughout
the year, awarded by the French Academy, ac-
cording to the will of Jean-Baptiste-Robert Auger,
Baron de Montyon, who bequeathed $60('.000 to
public hospitals, and the remainder of his fortune
to give sums of money to poor patients on leaving
Paris hospitals, and to found the prizes since con-
nected with his name. The Academy of Sciences
awards annually a prize of 10,000 francs to the in-
dividual who has discovered the means of making
any mechanical occupation more healthy, another
of equal value for improvements in medicine and
surgery; while the Forty themselves award the
prize of virtue, and another to the writer of the
work likely to have the greatest beneficial in-
fluence on morality — both alike of 10,000 francs a
year.
MOODY, DwiGHT Lymak. an American evangel-
ist, born at Northfield, Mass., Jan. 5, 1837. He was
for a while a salesman in Boston, and in 1856 went
to Chicago, where he engaged with remarkable
success in missionary worlT. In 1S70 he was joined
by Ira David Sankey, who was born at Edinburgh,
Pennsylvania, Aug. 28, 1840. In 1873 they visited
Great Britain as evangelists, attracting great
crowds, and afterwards worked together there and
in America. Mr. Moody is the founder of North-
field seminary, a flourishing Christian educational
institution located in his native town.
MOON, Mountains of the, have played a mys-
terious part in African geography since the days of
Ptolemy, who indicated them as containing the
sources of the Nile. Their exact position was not
known; they were generally figured on mediwval
maps as a high range crossing the entire continent
from Abyssinia to the Gulf of Guinea. As modern
enterprise has opened up the interior of Africa
different mountain-chains and peaks have been
identified as Ptolemy's Mountains of the ISIoon.
MOONWORT. an interesting fern, widely dis-
tributed over northern Europe, penetrating to
within the Arctic regions and Asia, and, with the
few other species of which the family is composed,
appearing also in North America.
MOORE. Benjamin, an American educator and
divine, born at Newtown, N. Y., Oct. 16, 1748. died
1100
M 0 0 11 II E A 1 ) — .M ( ) U J. !•: Y
in 1816. He was long connected as a minister with
Trinity church, New York City; became bishop in
1801 ; and was president of Columbia College from
1800 to 1811.
MOORHEAD, a city, the county-seat of Ulay
county, Minn., situated on Ked River. It contains
a State normal school.
MOORE, Frank, an American compiler and pub-
lisher, born in New Hampshire in 1828. He has
produced a number of valuable works relating!"
American history.
MOORE, George H., an American author an ',
librarian, born in New Hampshire in 1823. He hii ,
been librarian of the New York Historical Society
and of the Lenox Library, and has written a nunj
ber of historical works.
MOORE, Jacob Baii^by, an American writer ol
local histories, born in New Hampshire in 1797, died
in 1853. He became librarian of the New York
Historical Society in 1845, and was postmaster of
San Francisco from 1848 until his death.
MOOSE. See Britannica, Vol. VII, p. 24.
MORAN, Tiio.MAS, an American artist, born in
England in 1837, but came to Philadelphia while ii
child. His magnificent paintings The Grand Canon
of the Yellowstone and The Chasm of the Colorado
were bought by Congress for .'^20,000. His brother
Peter has devoted himself to the painting of ani-
mals, and his brother Edward to the production of
marine subjects.
MORANO, a city of southern Italy, built on a
hill in a wild neighborhood, 37 miles northwest of
Cosenza. Population, 8,259.
MORATA, Olympia Fulvia (1526-1555), an Italian
authoress.
MORAVIA, a village of Cayuga county, N. Y., 18
miles southeast of Auburn. Woolens, cheese, flour
and spokes are manufactured here, and the lousi-
ness of the surrounding region is largely dairying
and stock-raising.
MORAVIAN CHURCH. See Britannica, VoL
XVI, pp. 811, 812. See also Religious Denomina-
tions IN THE United St.vtes in these Revisions and
Additions.
MORELLA, a town of Spain, eight miles north of
Valencia. It was the stronghold of Cabrera, the
Carlist general, who scaled the castle Tan. 25, 1839.
It was re-taken in July, 1840, by Espartero. Popu-
lation, 7,190.
MORELOS, Jose Maria (r. 1765-1815), a Mexi-
can revolutionist, born about 1765. His birthplace,
Valladolid, was re-named Morelia in his honor. He
was the ablest of the leaders in the revolt of the
Mexicans against the Spaniards. He was taken
prisoner Nov. 15, 1815, borne in triumph to the city
of -Mexico and there shot.
MORENCI, a post-village of Lenawee county,
Mich. It contains a woolen factory and a flour
mill.
MORESNET, a small neutral territory, of about
seventy acres, between Belgium and Prussia, five
miles sotitli-west of Aix-la-Chapelle. There is on it
a village of 3,()0()inluiliilMnts.
MO R ETON- HAY CHESTNUT, a genus of plants
so namiMl because of the supposed resemblance in
form and qualities of the seeds to the sweet chest-
nut of Europe. It is a native of Australia. The
tree grows to the height of from seventy to one
hundred feet, with spreading branches clothed
with pinnate leaves about a foot long. The flowers,
bright yellow and red, are succeeded by cylindri-
cal pendulous pods of a bright brown color, six to
eight inches long.
MORGAN, Daniel, an American Revolutionary
general, born in New Jersey in 1736, died in 1802.
Congress voted him a gold medal for his victory at
the battle of Coupeiis. He rendered good service
in the suppression of the "whisky insurrection."
He was a member of Congress from 1795 to 1799.
MORGAN, Edwin Dennison, an American mer-
chant and statesman, born in Massachusetts in
1811, died in 1883. He Vjecame State senator of
New York in 1843, and governor in JS59. He
ranked as a major-general throughout the war,
and became United States Senator in 1863. He
twice declined the Secretaryship of the Treasury.
MORGAN, (teorge Wa.siiington, an American
soldier and statesman, born in Pennsylvania in
1820. He served with the Texan army of independ-
ence, in the Mexican war, and in the civil war. He
was the Democratic nominee for governor of Ohio
in 1865, and was a member of Congress from 1871
to 1875.
MORGAN, John Henry, a Confederate general
in the civil war, born in Alabama in 1826, died Sept.
4, 1864. He became known as a very bold and suc-
cessful raider, and his troops were known as "Mor-
gan's guerillas." He was surprised by Union cav-
alry at Greenville, Tenn., and killed while attempt-
ing to escape.
MORGAN, Lewis Henry, an American archaeol-
ogist, born at Aurora, New York, Nov. 21, 1818,
died Dec. 17, 1881. He graduated at Union College
in 1840, and became a lawyer at Rochester. He
served in the State assembly in 1861, and in the
senate in 1868. Morgan's earliest work. The League
of the Iroquois was the first account of the organi-
zation and government of an Indian tribe ; but
evenmore valuable are his SyMems of Con.ianguin.'tt/
md. Affinity of the Human Fainily. and his treatise
on Ancient Society.
MORGAN CITY, a post-village and port of entry
of St. Mary's parish, Louisiana, on .^tchafalaya
River, eighty miles southwest of New Orleans. It
has a good harbor and is connected by steamer-
lines with ports in Texas. Cuba, and Mexico. Pop-
ulation, 2,200.
MORGUE, a building in Paris, just behind the
cathedral of Notre Dime, where the dead bodies of
persons unknown, found either in the river (Seine)
or in tlie streets, are exposed to pul)lic view for
three days. The corpse is put under a glass case,
on sloping slabs of marble. When a corpse is iden-
tified, it is handed over to the relatives or friends
of the deceased, on payment of costs and dues;
otherwise it is interred at the expense of the city.
The number of bodies yearly exposed in the morgue
is about 300, tive-sixths of which are males. There
are morgues in Berlin, and in Boston, New Y'ork,
Brooklyn, Philadelphia, Chicago and otlier Ameri-
can towns. See Britannica, Vol. V. p. 331.
MORIKE, EniARD, a German poet, born in
Wiirtemburg, Sept. 8, 1804, died June 4, 1875.
MORISOX, James Cotter, an English author
and positivist, born in 1831, died Feb. 25. 1888. He
was educated at Highgate grammar-school and
Lincoln College, Oxford. His first work was his
masterpiece. The Life and Timet of St. Bernard.
His latest, T/if Serrice of ^fan. an E.ifay Toxeards
the Reliijion of the Future, attracted much attention,
but it was commenced when sickness had already
seized him, and it does not adequately represent
his views. He was one of the founders and first
proprietors of the "Fortnightly Review." His in-
tellectual gifts were associated with a most genial
and kindly nature ; he was reputed one of the best
talkers of his time in French as well as English,
and had long projected a work on the history of
France, Init owing to ill health it was never begun.
MORLEY, Henry, an English author, born in
London, Sept. 15, 1882, and educated at the Mora-
vian school, Neuwied-on-the-Khine, and King's Col-
M 0 R L ]'] V — M. ( ) 11 Jl 1 S
1101
lege, Ivondon, where lie edited the "King's College
Magazine." After pradicixig iiiedieiiic at -Madeley,
from 1S44 till 1848, and Iveepiiig scliool for liii' next
two years at Liscard, J-iverpuol, he settled down in
L(]ijdon to literary work in connection with ■'House-
hold Words" and the ••Kxaminer." Of the latter he
was joint-editor from Iholi to 185H, and sole editor
from lliat year till 1864. He was English lecturer
at King's College for eight years previous to 1865,
when he became professor of English language and
literature at University College, London. In 1870
he was appointed examiner in English language,
literature, and history to the university of London.
No other man has done so much to make classical
literature accessible to t^he people as Henry Mor-
ley through his admirajjle series, Moriei/s i'aiverxal
L(7jrflc.v, embracing sixtv-t'iree volumes; CaueU's
Natioiinl Library, 209 volumes, and the Carhhrooke
Library, a series of volumes issued in alternate
months.
MOKLEY, John, an English- writer and states-
man, born at Blackburn, Dec. 24, 18.38. He was edu-
cated at Cheltenham and Lincoln College, Oxford,
and, after taking his degree in 18.59, was called to
the bar, but chose literature as a profession. The
kest known of his books are Ethmind linrkc; Critical
.\fiiirrllnnirti; Voltaire; On (Jonijirniiiisr; Rousseau;
Dllcrol and tlv Encijdop^distx, and Rirhard Cobden.
From 1867 till 1882 he edited the ''Fortnightly Re-
view," and he has edited the "English Men of Let-
ters" series. He is an honorary LL. D. of Glasgow.
He unsuccessfully contested Blackburn in 1865,
and Westminster in 1880. From 1880 to 1883, when
he was elected for Newcastle-on-Tyne. Mr. ^lorley
was editor of the "Pall Mall Gazette." His articles
in favor of Home Rule written then, and followed
up by action in the house of commons and
speeches in the country in 1885, did much to influ-
ence public opinion before Mr. Gladstone's change
of |)olicy was known. In 1886 he became Irish sec-
retary till the dissolution which followed the rejec-
tion of the Home Rule bill in that year. In 1890,
during the difficulty as to the leadersliip of the
Irish party, he directly supported .Mr. Gladstone.
.MORfjEY, S.vMUEi., an English merchant and
l)hilantliropist, born at lloinerton, Oct. 15, 1809,
died Sept. 5, 18S6. He was returned to parliament
for Nottingham, in the Liberal interest, in 1865;
was unseated on petition ; represented Bristol,
1868-85, and declined a peerage which was oHered
to him in the latter year. He was identified with
many religious and philanthropic movements. He
gave $30,000 towards the erection of a Noncon-
formist memorial hall, and during 1864-70 con-
tributed $7(),tX)0 towards the erection of Congrega-
tional chapels.
MORLEY, Thomas (r. 1545-1604), an English
Composer. In 1601 he published the work by which
he is now known, r/ic Triumphs uf 0/v«««, being a
collection of 24 madrigals in honor of <2ueen Eliza-
beth, written by 24 Englishmen and set to music
by Morley.
MORMONS. On .Tan. 12, 18S7. the ll.)use of Rep-
resentatives passed without division a bill for the
suppression of polygamy in the Territory of Utah.
Its chief provisions are: (1) Polygamy is declared
to he a felony ; (2) The chief financial corporations
of the Mormons are dissolved, and the attorney-
general is directed to wind them up by process of
the courts; (3) Polygamists are made ineligible to
•vote; (4) AU voters in Utah are to be reijuired to
take an oath to obey the laws of the United States,
and especially the laws against polygamy ; (5)
Woman suffrage in Utah is abolished, and (6) Law-
ful wives and husbands are made competent wit-
nesses against persons accused of polygamy. It
was reported in September, 1890, that polygamy
had been declared to be no longer a feature of the
Mormon teaching, and that it was the intention of
the sect to submit to the ordinary laws binding on
Americans. See Britannica, Vol. Wl, pp. 825-
828.
MOROCCO. See under Lkatiier, Britannica,
Vol. XIV, pp. 3S8, 389.
MOROCCO. Eor general article see Britannica,
Vol. XVI, pp. 830-836. According to the most re-
cent investigation the area of the Sultan's do-
minions is about 219,000 English square miles. The
estimates of the population of Morocco vary from
2,500,000 to 9.400,000 ; it is generally considered lo
be about 5,000,000 souls, although Dr. Rohlfs, in the
"Geographische Jlittheilungen" (1883), maintains
that the ijopulation is not more than 2,750,000. An
estimate of 1S89 gives the following results: The
region of the old kingdom of Fez, 3,200,000; of Jlo-
rocco, 3,900,000; of Tafilet and the Segelmesa
country, 850,000; of Sus, Adrar and the Northern
Draa, 1,450,000; total, 9,400.000. Again, as to race:
Berbers and Tuaregs, 3,000,000; Sheila Berbers,
2,200,000; Arabs (1) pure nomadic Bedouins, 700,-
000 ; (2) 3Iued, 3,000,000 ; Jews, 150,000 ; negroes, 200,-
000. The number of Christians is very small, not
exceeding 1,500. Much of the interior of Morocco
is unknown to Europeans.
Phese.vt Reigning F.mhily .\nd Government. —
The present sultan is iMuley-Hassan, born in 1831.
eldest son of sultan SidioISlohamed. He ascended
the throne at the death of his father. Sept. 17,
1873. He is known to his subjects under the title
of "Emir-al-JIumenin," or Prince of True Believers.
He is the fourteenth of the dynasty of the Alides,
founded by JIuley-Achmet, and "the thirty-fifth
lineal descendant of Ali, uncle and son-in-law of
the Prophet.
The form of government of the sultanate, or em-
j>ire of Morocco, is in reality an absolute despotism,
unrestricted by any laws, civil or religious. The
sultan is chief of the state, as well as head of the
religion. As spiritual ruler, the sultan stands
([uite alone, his authority not being limited, as in
Turkey and other countries following the religion
of Mahomed by the expounders of the Koran, the
class of "Ulema," under the "Sheik-ul-Islam." "The
sultan has six ministers, whom he consults if he
deems it prudent to do so; otherwise they are
merely the executive of his unrestricted will. They
are the vizier, the ministers for foreign affairs
and home affairs, chief chamlierlain, chief treas-
urer and chief administrator of customs. The
sultan's revenue is estimated at $2,000,000 \nr
annum, derived from monopolies, taxes, tithes and
presents.
In 1.S83 the sultan granted the claim of Spain to
the small territory of Santa Cruz de ^Mar Peqnefia,
near the mouth of the Yfnu River, south of .Moga-
dor.
MORPHY, P.\ri, C, an American chess-player,
born in New Orleans, in 1837, died in 1884.
MORRIS, Chari.es, an American commodore,
born at Woodstock, Conn., in 1784, died at AVash-
ington, D. C, in 1856. He served with distinction
in the war with Tripoli and in the war of 1812. He
held many posts of responsibility in the navy de-
partment.
MORRIS, Ci..\,RA, an American actress, born in
1846 at Cleveland, Ohio. In 1874 she was married
to F. C. Harriott, of New York.
MORRIS, Francis Ori-en, an English author and
divine, born at Beverley in 1810. He took orders
in the Church of England, and became chaplain to
the duke of Cleveland. He has written many valu-
able works on natural history.
no-:
-M 0 RUT S — -M (> It TON
M OK Ills, Gi:oi:(iic I'lCKKiNs.aiitlnjr of " Woodman,
Spare that Tree,'' burn in I'hiludelpliia, Oct. lU,
1S02, died in New York. .July (i. ISW. He founded
llie New York "Jlirror" and al'terwards tlie "Home
.loiirnal." with both of wliii-h N. 1'. Willis was asso-
ciated.
MORRIS, tiEOROE Svi.vHsTKu.an American philo-
sophical writer and educator, liorn at Norwich, Vt.,
in 1840. He has lieen iirominently connected with
the University of Michigan and with the Johns-
Hopkins University.
ilORRIS, GouvEK.NEUR, an American statesman,
born in Morrisania, New York, Jan. 31,1752, died
Nov. 6, 1816. He graduated at King's (now Colum-
bia) College in 1768, and was admitted to the bar
in 1771. He took an active share in the political
affairs of the Revolutionary period. In May, 1780, he
lost a leg through a fall from his carriage in Phila-
delphia. From 1781 to 1784 lie was assistant to
Robert Morris, superintendent to the national
finance. In 1787 he took his seat as a delegate in the
convention that framed the United States Consti-
tution. The greater part of the year 1791 he spent
in England as a conlidential agent of Washington,
and next served till August. 1794, as United States
minister to France. Returning to America in 1798,
he sat for New York in the United States Senate
from ISOO to 1803. and was chairman of the New
York canal commissioners from 1810 till his death.
MORRIS, John G., an American clergyman,
educator and writer, born at Y'ork, Pa., in 1803.
He is the founder of the village of Lutherville, Md.,
and of the female seminary there located. He" is
prominently connected with many scientific and
other societies.
MORRIS, Lewis, one of the signers of the Dec-
laration of Independence, born at Jlorrisania, N.
Y., in 1726, died in 1798. He was a half-brother
of Gouverneur Morris.
MORRIS, Lewis, an American colonial gover-
nor, born at Jlorrisania, N. Y., in 1671, died in
1 746.
JMORRIS. Lewis, a popular English poet, born
in Carmarthen in 1832. He was educated at Sher-
liorne School and at Jesus College, Oxford, where
in 18.5.5 he graduated first-class in classics, and won
I lie Chancellor's prize. He was called six years
later to the English bar, and practiced till 1881,
when he accepted the post of honorary secretary
lothe university of Wales. His first offerings of
verse appeared in 1871, when under the pen-name
of "A New Writer" he published Sony.t cf Tii'o
W'irhh, which at once passed into numerous
editions, and which was followed by a second and
third volume. In 1.876 appeared T/ic /i'/^/o of //^rc/c.'!,
the work with which the author's name is usually
associated; it has run into several series, and
these series into many editions. He has since
published (■/"'(■//, (I Dnuim: The Ode of Life; Soiiij«
f'/i.sjuK/; (li/rl(i. It Tidii'ilii: and ,-1 Vision of Sal7its
(1890).'
MORRIS, Ri( ii.Mti), an English philologist, born
at Uermondsey in 1833. He is an active member
of the Chaucer and the Early English Societies,
and president (if the Philological Society. He has
written many valuable philological works, and ed-
ited iiunierous early texts.
.MoRlilS, Tii.!.MAs. a bishoii of the Methodist
Kpisciipal ('liuri'li. born In We<t Virginia in 1794,
(lied in I,S74.
.MORRIS, Wii.i.i^M. artist and poet, born at
Walthamstow in 1834, and educated at ^Marlborough
and Exeter College, Oxford. Mr. !\Iorris turned
his attention for some time to the study of archi-
tecture; and in 1.868. together with his friends
')ante G. Rossetti and Burne Jones, endeavored to
elev;ile the artistic taste of the public. For this
purpose a business of "art fabrics." uall-pajiers, and
stained glass, was started which has been extremely
successful. Mr. Morris published in 1867 his poem
Tlie Jjifi' and Death of Jason, which was followed in
1868-71) by The Earthly Paradise, a series of twenty-
four romantic tales. His later works include Lure
is Enough; Tlie Stonj of Siijurd Die Vohautj; and
Hopes and Fears for Art. He has recently trans-
lated the Odyssey of Homer, and in conjunction
with ilr. Eirikr Magnusson rendered into English
verse a number of Icelandic Stories. Mr. Morris
is one of the leaders of the socialistic movement in
England. A book by him entitled The OlilleriiKj
I'ldiii. appeared in 1890.
M0|;RIS, a city, the county-seat of Grundy
county. 111., one of the largest griiin-niarkets of the
West. It manufactures plows, cultivators, school
furniture, and carriages, and contains bituminous
coal-mines.
MORRIS, a post-village, a railroad junction and
the connty-seat of Stevens county, 51 inn., in the
western part of the State on Pomme de Terre
River, 159 miles northwest of St. Paul.
MORRISBURG, a town of Ontario, a port of en-
try, situated on the St. Lawrence, ninety-two miles
west of Montreal. It does an extensive shipping
business, and has a valualile water-power.
MORRISON, a city, the county-seat of White-
sides county, 111.. 127 miles west of Chicago. It
has several stores and mills.
MORRISTOWN, a village in St. Lawrence county,
N. Y'., opposite Brockville, Canada, on the St. Law-
rence River.
MORRISTOWN, a post-village, a railroad junc-
tion and the county-seat of Hamblen county,
Tenn., situated in a mineral region where varie-
gated marble is obtained. The town contains two
colleges.
MORRISVILLE. a post-village, the county-seat
of Madison county, N, \'., thirty miles southwest of
Utica. It is a hop-growing center.
MORSE, Edward S., an American naturalist,
born in Maine in 1838. He has been professor of
zoology in Bowdoin College and in Harvard L'ni-
versity ; has written several works on natural his-
tory, and is a popular scientiric lecturer.
MORSE, Jedediah, an American geographer,
father of the inventor of the telegraph, born in
Woodstock, Conn., Aug. 23, 1761, died in 1826. He
is best known as the author of Morse's Geoffrajihi/.
MoKTARA, Edgak. a Jewish boy whtj, in 1858.
was forcibly carried off from his parents by the or-
ders of the archbishop of Bologna on the plea that
he had, when an infant, been baptized into Christ-
ianity by a Roman Catholic maid-servant. The
manner of the boy's abduction, and the refusal of
the Roman Catholic authorities to give him up to
his parents, becoming known throughout Europe,
excited great iiulignation, more particularly in
England. P>iit the boy remained in the hands of the
Roman Catholic church, and became an Augustin-
ian monk.
MORTAR-VESSEL, a class of gunboat for
mounting sea-service mortars. The most ancient
form of mortar- vessel was the "bomb-ketch," con-
venient because of the length of deck without a
mast.
MORTON. GEORtiE. born at York, England, about
1585. He was an active promoter of immigration
among the Plymouth Colonists; and was the editor
of "IMourt's Relation." the first account published
in England of the planting of the colony.
MOUT()N. Henry, a distinguished .\merican
( chemist, born in New York t!ity in 1836. He has
i been a voluminous vv'riter on scientific subjects. He
^
M 0 R T 0 N — M 0 U N T DESERT I S L A N D
1103
uioaiiit- president of tlie Stevens Institute of Tech-
nology in 1(S70.
.M(')KT( )X, James St. Clair, an American military
en!{ineer. born in Philadelphia in l(S2!t. He was
killed in the assault on Petersburg, .June 17, 18l>4.
MOKTKX, Levi Parsons, vice-president of the
United States, born at Slioreliani, Vermont, May
1(>, 1824. He was first a country store-keeper's as-
sistant, then partner in a Boston firm of merchants,
and in 1863 founded banking-houses in Xew York
and London. In lS78and ISKO, he was returned to
Congress as a Republican; in 1881 to 1S85, he was
minister to France, and in 1888 he was elected
vice-president of the United States.
MOKTOX, XATiiA.siEt. (16I3-ltj8.5;. brother of
(ieorge. the Plymouth colonist. He wrote several
works on the early history of Xew England.
MORTOX, Oliver Perry, an eminent American
statesman, born in Indiana in l,S2::i, diedin 1877. He
was governor of Indiana during the civil war, and
became United States Senator in 18()7.
.MORTON, Samuai. George, a distinguished
.\merican phvsician and naturalist, born in Phila-
delphia, .Ian. 26, 1799, died .May 15, 1.S51. Hestudied
medicine in Philadelphia and Edinburgh, and in
1.S39 was appointed professor of anatomy in the
Pennsvlvania Medical College. Morton may be re-
garded as the first American who endeavored to
place the doctrine of the original diversity of man-
kind on the scientific basis. His great works are
Vrnnin Amerirann. and Crunia .Hyiiptiacn. His
museum of comparative craniology, in the academy
of natural sciences. Philadelphia, contains some
1..5(H) skulls, 9U0 of them human.
.MORTON, Thomas (<-.159()-f.]64r)), brought a
colony from England to Massachusetts in 1622. He
came into conflict with the Puritans on the question
of worldly amusements, and published a satire
called The Xnc Enr/linh Canit'in. which gives an ex-
cellent description of the country.
MORTON, Wii.i.iAM T., an American dentist,
born in Massachu.tetts in l.'<19. died in 1866. He
is distinguished as the discoverer of the use of
ether as in ana>sthetic.
MOSES. See Britannica, Vol. XVI, pp. 86tl-61.
MOSK\\'.\, a branch of the Oka. It rises in a
marsh in the east of .'-molensk, flows east to the
city of Moscow, and thence to the Oka. It is nav-
igable from its mouth to Moscow, except between
November and April, when it is generally frozen,
and is connected directly with the Volga by the
Mofkwa Canal.
MOSTAGANEJM, a town of Algeria, on the coast,
forty-five miles north-east of Oran. It manufac-
tures pottery and has corn-mills and tanneries.
Population in 1886, 12,39.5, more than one-third be-
iTig Europeans. It was a place of 40,000 in the 16th
century ; and has again grown up from its decayed
state since the French took possession in 1833.
MOTHE CADILLAC ANTOIXE. See Cadii-lac,
in these Revisions and Additions.
MOTIFF, in a musical composition, the princi-
pal subject on which the movement is constructed,
and which, during the movement, is constantly ap-
pearing in one or other of the parts, either com-
pletely or modified.
MOTT, l.,fCRETiA Coffin, an American philan-
thropist, born at Xantucket in 1793, died in 1880. In
1S19 she became a Quaker preacher, and thereafter
was known as an able advocate of peace and an
Dpposer of slavery.
.MOL'I D, or Mon.Di.vEss, the common name of
many minute fungi which make their appearance,
often in crowded multitudes, on decaying or diseased
plants and animals, and animal and vegetable sub-
stances. To the naked eye they often seem like
patches of fine cobweb, which are shown by the
microscope to consist of cellular threads.
MOULDING AND CA.STING. See Britannica,
Vol. IX, pp., 479-81.
MOULTON, Loi'isE Cha.ndler, an American
writer, born in Ponfret, Conn., April 5, 1835, mar-
ried at twenty W. U. Moulton, a Boston publisher,
and has published children's stories, novels, essays,
and poems. Her stories are unaflfected and well
constructed, full of grace and tenderness ; her verse
reveals the rarer gift of lyrical music. Here may
be named Brdthne .S7o/vV.v; Shuh' Woniin's Henrts, and
//( llie Garden of Diraiiis (1890), a volume of charm-
ingly tender and pathetic verse.
JIOULTON, a post-village, the county-seat of
Lawrence county, Ala. It contains a boys' acad-
emy and a girls' institute.
MOULTRIE. .Jou.v, an English poet, born in Lon-
don in 1799, died in 1874.
MOULTRIE, Fort, a fortress on Sullivan's Is-
land, at the mouth of Charleston harbor. South
Carolina, celebrated for the repulse of a British
squadron commanded by Sir Peter Parker, Jan. 28,
1776. The fort, which had 2() guns and 435 men,
and was commanded liy Colonel William Jloultrie
(1781-1805), had been hastily built of iialmettologs,
in two rows 16 feet apart, with the space between
filled with sand. The spongy wood of the palmetto
was found to resist the cannon balls perfectly.
MOI'LTRIE, William, an American military
commander, born in South Carolina in 1731, died
in 1805. He fought with distinction in the Revolu-
tionary war.
MOUND-BIRDS, a family of galinaceous birds
remarkable for the large mounds which they build_
as incubators for the eggs. They are natives of
Australasia and of the islands in the eastern arclii-
pelago and Pacific.
MOUND CITY, a post- village, the county-seat of
Pulaski county. 111., seven miles north of the mouth
of the Ohio river. It contains a national cemetery
and the western naval station.
;M0UXD CITY, a post-village, the county-seat of
Linn county, Kan., on Little Sugar Creek. It has
machine-shops, a foundry, and a system of water-
works.
MOUNDSVILLE, a post-village, the county-seat
of Marshall county, W. Va. It contains the State
penitentiary, several saw, woolen, and rolling-mills,
and a coal-bank. Here is situated the largest In-
dian mound in America.
.MOUNTAIN. George, a Canadian bishop, son of
Jacob Mountain, born in England in 1789, died in
1863.
MOUNTAIN, Jacob, a Canadian bishop, born in
England in 1750, died in 1825.
MOUNT AYR, a post-village, the county-seat of
Ringgold county, Iowa, in the southern part of the
State, near the West Fork of Grand River.
MOUNT CARMEL, a city, the county-«eat of
Wabash county. 111., on Wabash River. It con-
tains manufacturing establishments, flour and saw-
mills.
MOUNT CARMEL, a post-borough and a rail-
road junction of Northumberland county. Pa., con-
taining mines of coal. Population, 8,243.
MOUNT CLEMENS, a city, the county-seat of
Macomb county, Mich., twenty miles northeast of
Detroit. It contains lumber manufactories, a fur-
nace, and celebrated magnetic mineral springs.
Population, 4,742.
MOX'NT DESERT ISLAND, a mountainous
island, fifteen miles long and twelve miles wide,
south of Maine in the Aslantic (5cean. It contains
beautiful lakes and several villages and is a favor-
ite summer resort.
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